Stratno | Stratigraphic Name | Reference Id | Usage No |   Usage  | Page Number | Minimum Age Name | Maximum Age Name | Reference Comments | Numerical Age | Parent Units | Constituents | Related Units | Lithology | Last Update
77868|Abattoir East Gabbro|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||2960 - 2650 Ma (inferred).||||Gabbro; tholeiitic; differentiated; metamorphosed.|
77868|Abattoir East Gabbro|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2960-2650 Ma (inferred)||||Gabbro; tholeiitic; differentiated; metamorphosed|
77869|Abattoir West Gabbro|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||2960 - 2650 Ma (inferred).||||Gabbro; differentiated; metamorphosed.|
35663|Abbotshall Chert|23136|6|Mentioned|p265 Fig.1|||||||||
80523|Abdul Sandstone|13615|3|Fully described|p17, p4, p6-p8, p41-p42|Roadian|Kungurian|Peedamullah Shelf. Up to 50m thick. Spores and Pollen zone provided. Intersected by Abdul's Dam 1 drillhole wherein the type section is found between 707 and 747.5 m. Palynozone: D ericianus. Said to be Ufimian age. Previously called Nalbia  Sandstone in Ruby 1 (Mills, 1997). Also known from Onslow 1. Deposited in a marine shelf environment. See also p15,  p48, p62-p63, p81, p83, p85, 86, p103 App3, Paltes 2, 3..||Of Kennedy Group.||Conformably overlies the Ruby Limestone, Cody Limestone. Conformably overlain by the Chinty Formation. Conformably overlain by the Locker Shale.|Clear, translucent and milky white, fine- to medium-grained sandstone; rarely coarse grained, well-sorted, minor microcrystalline limestone.|07-FEB-19
27099|Abrakurrie Limestone|22587|6|Mentioned|p79 Fig.7|Early Miocene|Late Oligocene|||||||
27099|Abrakurrie Limestone|22626|2|Defined|437,439,441-443,447|Early Miocene|Late Oligocene|Geol province Eucla Basin. Max thickness 100-120 m||||||
27099|Abrakurrie Limestone|22814|6|Mentioned|p258|Tertiary|Tertiary|||||||
27099|Abrakurrie Limestone|23768|5|Briefly described|p28 Fig.5, p31, p41|Middle Miocene|Early Miocene|Overlies Wilson Bluff Formation, underlies Nullarbor Limestone. Maximum thickness: >30m.  See also p113.||||||10-MAR-05
27099|Abrakurrie Limestone|24057|5|Briefly described|p97|Early Miocene|Early Oligocene|Geological Basin: Eucla Basin.||||||
27099|Abrakurrie Limestone|24094|4|Described|p273|Early Miocene|Late Oligocene|Disconformbly overlies the Wilson Bluff Limestone and the Toolinna Limestone. Overlain by Nullabor Limestone. Geological Province: Eucla Basin||||||16-MAR-05
27099|Abrakurrie Limestone|24347|5|Briefly described|p114|Early Miocene|Late Oligocene|Geological Province: Eucla Basin.||||||
27099|Abrakurrie Limestone|29856|6|Mentioned|p37|||||||||
27099|Abrakurrie Limestone|30268|6|Mentioned|p43|||||||||
27099|Abrakurrie Limestone|30976|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
27099|Abrakurrie Limestone|31562|5|Briefly described|p13|||Early Miocene||||||
27099|Abrakurrie Limestone|31850|4|Described|p34|||Definition summary||||||
27099|Abrakurrie Limestone|31902|4|Described|Table 1|||Lower Miocene. Fig.1||||||11-JUL-13
27099|Abrakurrie Limestone|31903|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
27099|Abrakurrie Limestone|31907|4|Described|p8|||See also Table, Fig.1||||||
27099|Abrakurrie Limestone|31908|4|Described|Table 1|||L.Miocene||||||
27099|Abrakurrie Limestone|31909|3|Fully described|p8|||L.Miocene?||||||
27099|Abrakurrie Limestone|32552|2|Defined|p192|early Miocene|early Miocene|See also p193-199.||||||27-AUG-18
27099|Abrakurrie Limestone|32648|6|Mentioned|p32|||Tertiary||||||
27099|Abrakurrie Limestone|32750|4|Described|p305|||||||||
27099|Abrakurrie Limestone|32752|6|Mentioned|p337|||||||||
27099|Abrakurrie Limestone|34192|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
27099|Abrakurrie Limestone|34194|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
27099|Abrakurrie Limestone|34232|6|Mentioned|p76|||Cavities.||||||
27099|Abrakurrie Limestone|35059|6|Mentioned|Table.19|||||||||
27099|Abrakurrie Limestone|35097|6|Mentioned|p17|||||||||
27099|Abrakurrie Limestone|35772|6|Mentioned|p11|||||||||
27099|Abrakurrie Limestone|36200|6|Mentioned|p15|||||||||
27099|Abrakurrie Limestone|36257|6|Mentioned|Table 2.1|||||||||
27099|Abrakurrie Limestone|36890|3|Fully described|p415|||||||||
27099|Abrakurrie Limestone|37577|6|Mentioned|p75|||||||||
27099|Abrakurrie Limestone|38553|6|Mentioned|p43|||||||||
27099|Abrakurrie Limestone|38602|6|Mentioned|p2|||||||||
27099|Abrakurrie Limestone|40410|6|Mentioned|p3|||||||||
27099|Abrakurrie Limestone|40992|6|Mentioned|Fig.23|||||||||
27099|Abrakurrie Limestone|41043|6|Mentioned|p87|||||||||
27099|Abrakurrie Limestone|41075|6|Mentioned|p18|||||||||
27099|Abrakurrie Limestone|41076|6|Mentioned|p70|||||||||
27099|Abrakurrie Limestone|41505|6|Mentioned|p6|||||||||
27099|Abrakurrie Limestone|41519|6|Mentioned|p169|||||||||
27099|Abrakurrie Limestone|42335|4|Described|p325|early Miocene|late Oligocene|Also further description p327-339.||||||27-AUG-18
27099|Abrakurrie Limestone|42734|5|Briefly described|map legend|Tertiary||||||||
27099|Abrakurrie Limestone|43026|5|Briefly described|Table 4,p590|||||||||
27099|Abrakurrie Limestone|43040|5|Briefly described|p861|||||||||
27099|Abrakurrie Limestone|43203|5|Briefly described|Map Legend||Miocene|Eucla Basin||||||
27099|Abrakurrie Limestone|43498|5|Briefly described|8||Early Miocene|||||||
27099|Abrakurrie Limestone|43667|6|Mentioned|Fig.3,p12|Early Miocene|Late Oligocene|||||||
27099|Abrakurrie Limestone|43702|6|Mentioned|p405|Miocene|Oligocene|||||||
27099|Abrakurrie Limestone|43713|6|Mentioned|p2|||||||||
27099|Abrakurrie Limestone|44133|5|Briefly described|p183, 180 Fig. 10.22|Early Miocene|Late Oligocene|Geological Province: Eucla Basin. Overlies: Wilson Bluff Limestone. Thickness: 100m. ||||||
27099|Abrakurrie Limestone|44145|4|Described|p550, p556-7, p555 fig 4-194, p561|Early Miocene|Early Miocene|Eucla Basin south of railway.  Max thickness > 91m. Age from echinoid and foraminifera fauna. Type section: west wall of Abrakurrie Cave.||||Disconformably overlies Wilson Bluff Limestone. Disconformably overlain by Nullarbor Limestone.|Yellowish porous bryozoan calcarenite and granule calcirudite. Mostly grainstone with some packstone.|08-OCT-15
27099|Abrakurrie Limestone|44412|14|Not recorded|map legend||Early Miocene|L.Miocene.||||||
27099|Abrakurrie Limestone|45149|6|Mentioned|p62|||||||||
27099|Abrakurrie Limestone|45168|6|Mentioned|p6, Table 1|||||||||
27099|Abrakurrie Limestone|61155|6|Mentioned|p4|Late Oligocene|Late Oligocene|Geological Province: Eucla Basin.||||||
27099|Abrakurrie Limestone|61197|6|Mentioned|p489|Early Miocene|Late Oligocene|Eucla Basin.||||||
27099|Abrakurrie Limestone|61517|5|Briefly described|p309|Miocene|Oligocene|Unconformably overlain by Roe Calcarenite.||||||
27099|Abrakurrie Limestone|62369|5|Briefly described|p409, p410 Fig.4|Early Miocene|Oligocene|Coarse-grained bryozoan calcarenite, distinctly cyclic, and contains numerous hardgrounds; locally dolomitised. Overlain by the Nullarbor limestone. Geological Province: Eucla Basin.||||||
27099|Abrakurrie Limestone|62640|5|Briefly described|p68, pp70-77.      |Early Miocene|Late Oligocene|Up to 100m thick. High porosity and permeability. |c.26 - c.24 Ma.|||Overlies Wilson Bluff Limestone. Is overlain by Nullarbor Limestone.|Metre-scale subtidal cycles capped by thin marine hardgrounds, forming well-lithified layers in otherwise friable carbonate.|
27099|Abrakurrie Limestone|64646|6|Mentioned|p23 Fig. 3, p24 Fig. 4|Early Miocene|Late Oligocene|Geological Province: Eucla Basin.||||||08-FEB-10
27099|Abrakurrie Limestone|65942|2|Defined|p76||Miocene|1967 Annual Report. ||Of Eucla Group.||||
27099|Abrakurrie Limestone|66131|6|Mentioned|p242 Fig.2|Miocene|Oligocene|Late Oligocene to Early Miocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||||||
27099|Abrakurrie Limestone|67462|5|Briefly described|Map legend.|Miocene|Oligocene|Bunda Plateau, Eucla Basin.||||||
27099|Abrakurrie Limestone|67789|5|Briefly described|p34-35, 39-40, 45-46|Miocene|Oligocene|Eucla Basin. Up to 100m thick.||Eucla Group.||Overlies Wilson Bluff Limestone. Is overlain by Nullarbor Limestone.|A grainy neritic, bryozoan-rich, cool-water carbonate; contains numerous hard-grounds.|
27099|Abrakurrie Limestone|68715|6|Mentioned|p30 Fig.5|Aquitanian|Chattian|Bunda Plateau, Eucla Basin. ||||||
27099|Abrakurrie Limestone|69386|5|Briefly described|p7|Miocene|Oligocene|Eucla Basin.||||Overlies Wilson's Bluff Limestone.|Cool-water carbonate.|
27099|Abrakurrie Limestone|69598|5|Briefly described|p2, p9, p10, p11 Tb.1, p29 Tb.4|Early Miocene|Late Oligocene|Eucla Basin. Up to 120m thick. Potential carbon dioxide storage reservoir.||||Overlain by the Nullarbor Limestone.|Locally dolomitised coarse-grained bryozoan calcarenites and calcirudites.|
27099|Abrakurrie Limestone|69632|6|Mentioned|p26|Miocene|Oligocene|||Eucla Group|||Cool-water carbonate.|09-OCT-18
27099|Abrakurrie Limestone|69648|6|Mentioned|p25|||Deposited in cool to temperate waters on a platform that was drowned for part of the time, in central and southern parts of Eucla Basin (Lowry 1970; James and Bone, 1991). Age: Oligocene?||||||
27099|Abrakurrie Limestone|70397|5|Briefly described|p1-3|Early Miocene|Late Oligocene|Eucla Basin. Depositional environment: cool-temperate, open-marine shelf.||Unit of Eucla Group.||Unconformably overlain by Nullabor Limestone. Unconformably underlain by Wilson Bluff Limestone.|Medium- to coarse-grained bryozoan facies.|29-JUL-19
27099|Abrakurrie Limestone|70771|4|Described|p3-p4, p7-p8, p11-p12|Early Miocene|Late Oligocene|Eucla Platform, Eucla Basin. Seperated into two informal units (discussed p3). This unit is fossiliferous and contains abundant bryozoans, foraminifera, bivalves, brachiopods and echinoids; serpulid worms, solitary corals, gastropods and coralline algae also occur. This unit has a maximum thickness of up to 90m; however, a greater original thickness to the south has been suggested (Lowry, 1967). Interpreted to have been deposited on a shallow, open shelf with water depths up to 100m.   [The author assigns this unit to the Eucla Group however this term is obsolete]. See also p27, p31, p53-p58, p60-p61.||Eucla Group||Disconformably overlies the Wilson Bluff Limestone. Disconformably overlain by the Nullarbor Limestone and the Roe Calcarenite.|Moderately well-sorted, thin-bedded, friable fossiliferous calcarenite and indurated and thick-bedded calc-arenite.|
27099|Abrakurrie Limestone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||calcirudite, calcarenite|
27099|Abrakurrie Limestone|71361|4|Described|p5, p15, p17, p23|Early Miocene|Late Oligocene|Eucla Basin.  [NB The author assigns this formation to the disused Eucla Group on the basis of references to older literature - Lowry 1970]. Interpreted to have been deposited in a cool water, neritic envrionment. See also  p119, p140, p144, p192-p195.||Eucla Group||Unconformably overlies the Wilson Bluff Limestone. Unconformably overlain by the Nullarbor Limestone.|Medium to coarse grained, bryozoan grainstone to packstone with local fine-gained wackestone and coarse-grained floatstone and rudstone.|
27099|Abrakurrie Limestone|71618|6|Mentioned|p124|Cenozoic|Cenozoic|Geological province: Eucla Basin.||Unit of Eucla Group.||||05-SEP-19
27099|Abrakurrie Limestone|71891|5|Briefly described|p7|Cenozoic|Cenozoic|Eucla Basin. Thin (generally <10m thick) unit that is interpreted to have been deposited on a partly to completely drowned platform.||||Overlain by the Nullarbor Limestone. Overlies the Wilsons Bluff Limestone.|Limestone.|
27099|Abrakurrie Limestone|72344|5|Briefly described|p5|||Eucla Basin. Generally less than 10m thick. Forms a distinct yellow-brown band in the Bunda Cliffs.||||Overlies the Wilson Bluff Limestone. Overlain by the Nullarbor Limestone.|Yellowish coarse-grained bryozoan calcarenite and calcirudite, distinctly cyclic and contains numerous hardgrounds; locally dolomitized.|
27099|Abrakurrie Limestone|72465|5|Briefly described|p9|Tertiary|Tertiary|Eucla Basin, Coompana Province. Generally thin (<10m thick) unit. Forms a distinctive yellow-brown band in the Bunda Cliffs. Partly to completely drowned platform deposits.||||Overlies Wilson Bluff Limestone. Is overlain by Nullarbor Limestone.|Yellowish coarse-grained bryozoan calcarenite and calcirudite, distinctly cyclic, and contains numerous hardgrounds; locally dolomitized.|
27099|Abrakurrie Limestone|72466|5|Briefly described|p9|Tertiary|Tertiary|Benbow et al. (1995). Eucla Basin, Coompana Province. Generally thin (<10m thick). Deposited on a partly to completely drowned platform. Forms a distinct yellow-brown band in the Bunda Cliffs.||||Overlies Wilson Bluff Limestone. Is overlain by Nullarbor Limestone.|Yellowish coarse-grained bryozoan calcarenite and calcirudite, distinctly cyclic, and contains numerous hardgrounds; locally dolomitized.|
27099|Abrakurrie Limestone|72467|5|Briefly described|p9|Tertiary|Tertiary|Eucla Basin, Coompana Province. Generally thin (<10m thick) unit. Forms a distinctive yellow-brown band in the Bunda Cliffs. Partly to completely drowned platform deposits.||||Overlies Wilson Bluff Limestone. Is overlain by Nullarbor Limestone.|Yellowish coarse-grained bryozoan calcarenite and calcirudite, distinctly cyclic, and contains numerous hardgrounds; locally dolomitized.|
27099|Abrakurrie Limestone|72468|5|Briefly described|p9|||Eucla Basin. Thin; generally less than 10 m thick. Deposited on a partly to completely drowned platform. Forms a distinct yellow-brown band in the Bunda Cliffs.||||Underlain by Wilson Bluff Limestone. Overlain by Nullarbor Limestone.|Yellowish coarse-grained bryozoan calcarenite and calcirudite, distinctly cyclic, and contains numerous hardgrounds; locally dolomitized.|
27099|Abrakurrie Limestone|72469|5|Briefly described|p9|||Eucla Basin. Thin; generally less than 10 m thick. Deposited on a partly to completely drowned platform. Forms a distinct yellow-brown band in the Bunda Cliffs.||||Underlain by Wilson Bluff Limestone. Overlain by Nullarbor Limestone.|Yellowish coarse-grained bryozoan calcarenite and calcirudite, distinctly cyclic, and contains numerous hardgrounds; locally dolomitized.|
27099|Abrakurrie Limestone|72470|5|Briefly described|p9|||Eucla Basin. Thin; generally less than 10 m thick. Deposited on a partly to completely drowned platform. Forms a distinct yellow-brown band in the Bunda Cliffs.||||Underlain by Wilson Bluff Limestone. Overlain by Nullarbor Limestone.|Yellowish coarse-grained bryozoan calcarenite and calcirudite, distinctly cyclic, and contains numerous hardgrounds; locally dolomitized.|
27099|Abrakurrie Limestone|72471|5|Briefly described|p9|||Eucla Basin. Thin; generally less than 10 m thick. Deposited on a partly to completely drowned platform. Forms a distinct yellow-brown band in the Bunda Cliffs.||||Underlain by Wilson Bluff Limestone. Overlain by Nullarbor Limestone.|Yellowish coarse-grained bryozoan calcarenite and calcirudite, distinctly cyclic, and contains numerous hardgrounds; locally dolomitized.|
27099|Abrakurrie Limestone|72472|5|Briefly described|p9|||Eucla Basin. Thin; generally less than 10 m thick. Deposited on a partly to completely drowned platform. Forms a distinct yellow-brown band in the Bunda Cliffs.||||Underlain by Wilson Bluff Limestone. Overlain by Nullarbor Limestone.|Yellowish coarse-grained bryozoan calcarenite and calcirudite, distinctly cyclic, and contains numerous hardgrounds; locally dolomitized.|
27099|Abrakurrie Limestone|73084|6|Mentioned|p16|Miocene|Oligocene|||||||
27099|Abrakurrie Limestone|73641|5|Briefly described|p5|Miocene|Oligocene|Eucla Basin. <10m thick. Drowned platform environment.||||Overlies Wilson Bluff Limestone. Is overlain by Nullarbor Limestone.|Yellowish coarse-grained bryozoan calcarenite and calcirudite, containing numerous hardgrounds; locally dolomitized.|
37149|Abydos Monzogranite|23755|5|Briefly described|p18 Table 2|Archean|Archean|||||||07-NOV-08
37149|Abydos Monzogranite|24554|4|Described|p5 Tb.1, p8|Archean|Archean|Of the Yule Granitoid Complex. Age: c. 2945-2930 Ma. Geological Province: East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
37149|Abydos Monzogranite|50146|5|Briefly described|Map Legend|Archean|Archean|Of the Yule Granitoid Complex. Geological Province: Pilbara Craton. Porphyritic feldspar-quartz-biotite-titanite monzogranite; moderaltey to strongly foliated; metamorphosed||||||07-NOV-08
37149|Abydos Monzogranite|50379|5|Briefly described|Map Legend|Archean|Archean|Of Yule Granitoid Complex. Geological Province: Pilbara Craton.||||||07-NOV-08
37149|Abydos Monzogranite|61252|6|Mentioned|p67 Tb.1|||Of the Yule granitoid complex.||||||
37149|Abydos Monzogranite|63441|5|Briefly described|p10 Tb. 2|Archean|Archean|Of Sisters Supersuite. Geological province: Pilbara Craton.||||||07-FEB-11
37149|Abydos Monzogranite|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Unit in Sisters Supersuite. Feldspar(-quartz) porphyritic, biotite-titanite metamonzogranite; moderate to strong foliation.||||||15-DEC-22
37149|Abydos Monzogranite|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.||Of the Sisters Supersuite.|||Feldspar(-quartz) porphyritic, biotite-titanite metamonzogranite; moderate to strong foliation.|30-APR-14
37149|Abydos Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Sisters Supersuite|||Feldspar(--quartz) porphyritic, biotite--titanite metamonzogranite with abundant greenstone and granitic gneiss xenoliths; modertately to strongly foliated.|
37149|Abydos Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; North Pilbara Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|2954-2919 Ma (inferred)|Unit of Sisters Supersuite.|||Feldspar(-quartz) porphyritic, biotite-titanite metamonzogranite|
37149|Abydos Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
37149|Abydos Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Sisters Supersuite|||Porphyritic biotite--titanite metamonzogranite; feldspar and quartz phenocryts; moderate to strong foliation.|
68671|Abyssinia Well Orthogneiss|63441|2|Defined|p46 Appx.1, p7 Tb. 2|Archean|Archean|Of the Tambina Supersuite. Age: 3425+/-4Ma. Geological province: Pilbara Craton. Foliated to weakly gneissic, medium-grained to weakly porphyritic, blue-grey tonalite through monzogranite; commonly marked by lit-par-lit sheets of white leucogranite.||||||07-FEB-11
72737|Acacia Sandstone Member|62982|5|Briefly described|p7|Ordovician|Ordovician|Of the Willara Formation.  Potential reservoir. Geological Province: Canning Basin.||||||16-JAN-07
72737|Acacia Sandstone Member|64334|5|Briefly described|p39, 41, 43-46|Ordovician|Ordovician|Canning Basin; subsurface only. Arenig. Detrital zircon analyses and plots; ages and provenances discussed.||Willara Formation.||Is enclosed within Willara Formation. A likely correlative of the topmost Gap Creek Formation.|Sandstone.|
72737|Acacia Sandstone Member|65301|5|Briefly described|p3, p8 Fig. 5|Middle Ordovician|Middle Ordovician|Of the Willara Formation locally. Geological province: Canning Basin.||||||23-FEB-10
72737|Acacia Sandstone Member|65449|6|Mentioned|p3-5|||Local siliciclastics extending into the Basin during times of relative low stand of sea level.||Of Willara Formation.||||08-APR-20
72737|Acacia Sandstone Member|69182|6|Mentioned|Ch4 p9, Ch4 p38, Ch4 p39|||Canning Basin. Good porosity and permeability makes this a suitable candidate to be a reservoir for carbon dioxide storage, however the unit is generally thin and difficult to target. See also Ch4 p44, Ch4 p92-p96.||Willara Formation|||Reservoir sandstones.|
72737|Acacia Sandstone Member|71171|6|Mentioned|p2|||Canning Basin.||Willara Formation.||||
72737|Acacia Sandstone Member|73344|5|Briefly described|p6, p8|Dapingian|Dapingian|Canning Basin, subsurface. Part of supersequence A1. Underlain by Nambeet Formation in some places with apparent conformity.||Willara Formation||Underlain by Nambeet Formation.||
72737|Acacia Sandstone Member|73346|6|Mentioned|p27, App.1 p34|||Canning Basin. Shallow marine sandstone.||Willara Formation||||
77940|Agnew Komatiite|69586|5|Briefly described|p10-11, p13|||Agnew-Lawlers area. A prominent unit that outlines the Lawlers Anticline and the Mount White Syncline. Thickness varies considerably. Hosts gold mineralisation (Cox Crusader and Deliver deposits).||||Overlies Never Can Tell Formation. Equivalent to Kambalda Komatiite.|Relatively massive, medium-grained, equigranular, olivine-spinifex-textured, cumulate ultramafic rock; extensive carbonate and serpentinite alteration.|
77940|Agnew Komatiite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2720 - 2680 Ma (inferred).|Two Sisters Subgroup|||Komatiitic basalt; metamorphosed. Komatiite and komatiite flow units; olivine-spinifex texture and local well developed cumulate zones; metamorphosed.|
77940|Agnew Komatiite|70326|3|Fully described|p335-6,338,341-2,347-9, p354, p364|Neoarchean|Neoarchean|Geological province: Agnew region, Ora Banda Domain, Kalgoorlie Terrane, Yilgarn Craton. Thick cumulate lower sequence and an overlying stacked sequence of subaqueous komatiite flows. Produced during ~2705 Ma komatiite eruption event. Compositional characteristics are most similar to uncontaminated Al-undepleted (Munro-type) komatiites that are typical of the Neoarchean (Arndt et al., 2008). Thickness: 100m. Observed in many drillholes on western limb of Agnew Anticline, in outcrop in Mount White Syncline. Lithofacies include spinifex dominated upper half (?50 m), cumulate lower half (?50 m), and fragmental komatiite (<8 m). Major and trace element geochemical analysis on Table 4 p342-346. Marks the beginning of Cycle 2 Agnew greenstone Belt volcanism. Correlable to Siberia Komatiite and Cliffs Ultramafics. Cumulates can be correlated to Silver Lake Peridotite. See also p351,353-4,360,363-5.|~2705 Ma|||Overlain by Burrell Well Basalt. Underlain by Never Can Tell Basalt.|Spinifex-orthocumulate (1m thick komatiite sheet flows), massive ultrabasic cumulate (intrusion?). Fragmental Komatiite commonly at top contact. Subaqueous komatiite flows (and comagmatic intrusion?); fragmental komatiite interpreted as cataclasite.|29-JUL-19
77940|Agnew Komatiite|70863|6|Mentioned|p16|||||||||
77940|Agnew Komatiite|71212|4|Described|intro p2, intro p3, p1|||Yilgarn Craton. Up to 1500m thick. This unit is highly magnetic and hosts gold mineralisation where it contacts the underlying tholeiitic metabasalt. See also p46, p47, p53, p54, p61, p88, p108, p129, p136, p138, p148, p164, p204, p209, p234, p247, p248, p256, p257. ||Two Sisters Subgroup||Overlies the Never Can Tell Basalt. Overlain by the Claudius Member of the Scotty Creek Formation. Lateral equivalent of the Mount Keith Ultramafic Unit.|Serpentinised komatiite.|
77940|Agnew Komatiite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2711-2687 Ma (inferred)|Unit of Two Sisters Subgroup.|||Komatiite basalt; metamorphosed, komatiite; olivine-spinifex texture and locally well developed cumulate zones; metamorphosed|
77940|Agnew Komatiite|72057|6|Mentioned|p238|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton.||||||
77940|Agnew Komatiite|73151|5|Briefly described|p3, p5, p9, p10 Fig.6, p12-13|Neoarchean|Neoarchean|Yilgarn Craton. Kalgoorlie Terrane, Agnew Greenstone Belt.||Kalgoorlie Group||Overlies Never Can Tell Basalt, underlies Burrell Well Basalt, Redeemer Dolerite.|Komatiite.|
77940|Agnew Komatiite|73596|5|Briefly described|p1152, 1156-1158, 1160, 1162-1163|Neoarchean|Neoarchean|Agnew-Wiluna Greenstone Belt. Deep-water mafic-ultramafic lava fields and feeder intrusions.|2727 +/- 7 Ma.|Two Sisters Subgroup.||Overlies Never Can Tell Basalt. Is overlain by Burrell Well Basalt. Lateral equivalent to Perseverance Ultramafic Unit.||
30154|Ahern Formation|22547|3|Fully described|p27||Cryogenian|Geological province: Victoria River Basin. Previously Boll Sandstone. Age: c. 800 Ma. 200 m thick. Overlies Lamboo Complex, overlain by Helicopter Siltstone.||||||15-DEC-08
30154|Ahern Formation|22754|5|Briefly described|p11 Tb. 3|Mesoproterozoic|Mesoproterozoic|Geological Province: Victoria River Basin.||||||
30154|Ahern Formation|23314|6|Mentioned|333|||||||||
30154|Ahern Formation|23809|5|Briefly described|p47 Fig. 42|Proterozoic|Proterozoic|Geological Province: Victoria Basin.  Correlates with Auvergne Group (Victoria Basin), Renner Group (Ashburton Province) and the Roper Group (McArthur Basin).||||||09-NOV-04
30154|Ahern Formation|24122|6|Mentioned|p1|||||||||
30154|Ahern Formation|24297|6|Mentioned|p4|||||||||
30154|Ahern Formation|24503|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Geological Province: Victoria River Basin.||||||
30154|Ahern Formation|43853|5|Briefly described|Map Legend||Proterozoic|||||||
30154|Ahern Formation|43855|5|Briefly described|Map Legend||Proterozoic|||||||
30154|Ahern Formation|44230|5|Briefly described|Map Legend||Proterozoic|||||||
30154|Ahern Formation|44868|5|Briefly described|Map Legend||Phanerozoic|||||||
30154|Ahern Formation|60682|6|Mentioned|6|||Correlated with Jasper Gorge Sandstone.||||||
30154|Ahern Formation|60685|6|Mentioned|p4|||Mentioned in the context of the Ahern Formation-Helicopter Siltstone (east Kimberley) possible correlation with Jasper Gorge Sandstone-Angalarri Siltstone.||||||
30154|Ahern Formation|63866|5|Briefly described|p130|||Victoria River Basin.||||||
30154|Ahern Formation|64104|6|Mentioned|p63 Fig.1||||c.800 Ma.|||||
30154|Ahern Formation|64580|4|Described|map legend|Neoproterozoic|Neoproterozoic|Sandstone, pebbly sandstone, conglomerate, siltstone, and mudstone.||||||15-DEC-08
30154|Ahern Formation|68733|6|Mentioned|p190|||Wolfe Basin.||||||
30154|Ahern Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Neoproterozoic|Neoproterozoic|Victoria River Basin|||||Fine- to coarse-grained quartz sandstone; minor pebbly sandstone, conglomerate, and siltstone.|30-JUL-15
30154|Ahern Formation|69165|4|Described|100k_interpgeop_lut.csv|Neoproterozoic|Neoproterozoic|See also 500k_geologyp08_lut.csv.|||||Fine to coarse grained quartz sandstone; minor pebbly sandstone, conglomerate and siltstone.|
30154|Ahern Formation|69634|4|Described|GEOL_LUT_CSV files|Neoproterozoic|Neoproterozoic|Of Victoria River Basin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|1000-541 Ma (Inferred)||||Fine- to coarse-grained quartz sandstone; minor pebbly sandstone, conglomerate, and siltstone|
30154|Ahern Formation|70154|4|Described|100k_interpgeop_lut.csv, |Cryogenian|Cryogenian|See also 500k_interpgeop_lut.csv.|635-850 Ma||||Fine to coarse grained quartz sandstone; minor pebbly sandstone, conglomerate and siltstone.|
30154|Ahern Formation|71267|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Of Victoria Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|1000-720 (inferred)||||Fine- to coarse-grained quartz sandstone; minor pebbly sandstone, conglomerate, and siltstone|
30154|Ahern Formation|72034|5|Briefly described|500k_interpgeop16_lut|Tonian|Tonian|Victoria Basin.|||||Fine- to coarse-grained quartz sandstone; minor pebbly sandstone, conglomerate, and siltstone.|
24150|Airport Creek Formation|36483|2|Defined|p67-68|Pleistocene|Pleistocene|Unconformable on Mowanjum Sand. Av.exposed thickness: >3m. Geol.Prov: Canning Basin. Grey to buff, semi-lithified to indurated suite of sand (predominant), silt and burrow-structured to bioturbated sand, silt+clay; interlayered and interlaminated; fossils||||||07-AUG-07
24150|Airport Creek Formation|37615|5|Briefly described|Table 1|||||||||
24150|Airport Creek Formation|38013|6|Mentioned|Fig.3|||||||||
31387|Ajana Formation|1943|2|Defined|p382-384, p373, p375 Fig.3, p376 Fig 4|Ludlow|Late Ordovician|New name. Type section in Yaringa-1, 1271-1526m. Informally divided into lower, middle and upper cycles. Max. thickness: 317m in Dirk Hartog-17B (983-1400m)[probable error here: this interval is 417 m]. Base of Ajana Formation is a type 1 sequence boundary.||Dirk Hartog Group||Overlies eroded top of Tumblagooda Group. Correlated with upper Carribuddy Group, Canning Basin. Unconformbly overlain by Faure Formation (in Wandagee-1).|Multicoloured siltstone and shale at base; dolomitic and 'salty'. Grades up to shaly dolostones. Ooid limestones and dolostones in upper cyles.|20-JUN-13
31387|Ajana Formation|6943|4|Described|p599-606, p608.|Silurian|Late Ordovician|Upper part contains Llandovery conodonts. Middle part contains Teriodontus elements.||Unit at base of Dirk Hartog Group.|Includes Marron Member.|Is overlain by Yaringa Formation.|A shoaling carbonate unit with a distinctive basal siliciclastic member.|23-SEP-15
31387|Ajana Formation|12729|4|Described|p.4, 5, 10, 32; Figs. 8, 9, 23|||Type section ~1300-1526 m in Yaringa 1, Mory et al. (1998b) redefined after Gorter et al. (1994). Thickens to NW. Deposition in playa lakes with occasional marine incursions. Includes: Aphelognathus sp. aff. A. pyramidalis, a late Llandovery conodont fauna, and coniform elements (Teridontus sp. nov.).||Dirk Hartog Group|Marron Member|Underlies the Yaringa Formation.|Grey sandy mudstone, laminated dolomitic mudstone, and wackestone  with a distinctive basal siliciclastic member. Minor thin beds of very fine grained sandstone show current and wave ripples.|
31387|Ajana Formation|13995|5|Briefly described|p103|Early Silurian|Early Silurian|Carnarvon Basin. Age from a conodont assemblage.||||Overlies Tumblagooda Sandstone.||
31387|Ajana Formation|14228|5|Briefly described|p4, p5 fig2, p6 fig3|Llandovery|Llandovery|Gascoyne Platform. Contains Telychian conodont faunas.||Dirk Hartog Group|Marron Member|Overlies Tumblagooda Sandstone. Is overlain by Yaringa Formation.|Basal oxidized siltstone overlain by shoaling-up cycles of grey sandy mudstone, laminated dolomitic mudstone, and wackestone.|
31387|Ajana Formation|23572|4|Described|p10|Silurian|Silurian|Geological Province: Carnarvon Basin. Basal unit of the Dirk Hartog Group. Max. thickness: 435m. Overlying unit: Yaringa Formation.||||||
31387|Ajana Formation|23935|4|Described|p11 Fig.7|Llandovery|Ashgill|Of Dirk Hartog Group. Conformably overlies Tumblagooda Sandstone. Conformably overlain by Yaringa Formation. Geological Province: Southern Carnarvon Basin.||||||
31387|Ajana Formation|24581|6|Mentioned|p823|||Contains early Silurian conodonts.||||||
31387|Ajana Formation|43566|6|Mentioned|Fig.2,p415|||||||||
31387|Ajana Formation|49942|4|Described|p4 Fig.3, p9|Llandovery|Ashgill|Overlies Tumblagooda Sandstone. Conformably overlain by Yaringa Formation. Of Dirk Hartog Formation. Shallow marine. Geological Province: Gascoyne Platform.||||||
31387|Ajana Formation|50084|4|Described|p77, 78|Silurian|Late Ordovician|Thickness: 125 m. Overlies Tumblagooda Sandstone (conformable). Overlain by Yaringa Formation (conformable) and Coburn Formation. Of Dirk Hartog Group . Geological Province: Southern Carnarvon Basin.||||||07-FEB-11
31387|Ajana Formation|60384|6|Mentioned|p243 Fig 2a|Llandovery|Late Ordovician|Shown as Ashgill to Llandovery age||Of Dirk Hartog Group||||
31387|Ajana Formation|60725|5|Briefly described|p28, p29 Fig.2. |Silurian|Late Ordovician|Locally, moderate to good petroleum source potential.||Unit in Dirk Hartog Group.|||Carbonate-shales facies.|
31387|Ajana Formation|65313|6|Mentioned|p578, p579|||Carnarvon Basin.||Of Dirk Hartog Group.|Includes Marron Member.|Overlies Tumblagooda Sandstone.||26-MAR-12
31387|Ajana Formation|65449|5|Briefly described|p34|Llandovery|Llandovery|Southern Carnarvon Basin. Age from conodonts.||Dirk Hartog Group.||Conformably? overlies Tumblagooda Sandstone. Is overlain by Yaringa Formation.|Shoaling upwards cycles in grey sandy mudstone, laminated dolomitic mudstone, and wackestone.|
31387|Ajana Formation|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.||Dirk Hartog Group|Includes Marron Member.||Includes blue/grey (light and dark laminations) dolomitic claystone.|
31387|Ajana Formation|67200|6|Mentioned|p18 table 1, p46, p52, p56|||Thermal conductivity of 2.78 W/mK||Dirk Hartog Group|Includes Marron Member||Dolomitic claystone.|
31387|Ajana Formation|69297|6|Mentioned|p246, p249|Silurian|Ordovician|Gascoyne Sub-basin of the Carnarvon Basin.||Dirk Hartog Group||Overlies the Tumblagooda Sandstone. Overlain by the Yaringa Formation.||
31387|Ajana Formation|71146|5|Briefly described|p6|Llandovery|Late Ordovician|Southern Carnarvon Basin.||Dirk Hartog Group||Overlies the Tumblagooda Sandstone. Overlain by the Yaringa Formation.|Carbonate and mudstone.|
41023|Alabama Sandstone|24196|6|Mentioned|p47 Fig.5|||Geological Province: Laverton domain, Yilgarn Craton. See also Alabama sandstone.||||||25-MAY-04
24651|Albert Edward Group|22440|5|Briefly described|p5||Neoproterozoic|||||||
24651|Albert Edward Group|22496|4|Described|p11|Neoproterozoic|Neoproterozoic|Comprises the Mount Forster Sandstone, Elvire Formation, Boonall Dolomite, Douri Sandstone, Timperley Shale, Nyuless Sandstone and the Flat Rock Formation. Overlies the Ranford Formation.||||||
24651|Albert Edward Group|22547|3|Fully described|p28||Neoproterozoic III|Geological province: Wolfe Creek Basin. Age: c. 610 Ma.||||||14-NOV-06
24651|Albert Edward Group|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
24651|Albert Edward Group|22754|5|Briefly described|p10|Neoproterozoic|Neoproterozoic|Age c. 610 Ma.  Geological Province: Wolfe Creek Basin.||||||
24651|Albert Edward Group|22777|5|Briefly described|Map|||Wolfe Basin||||||
24651|Albert Edward Group|23216|5|Briefly described|p36||Vendian|Age by Rb-Sr whole rock.||||||
24651|Albert Edward Group|23314|6|Mentioned|329|||||||||
24651|Albert Edward Group|23328|5|Briefly described|1031 Fig.2|Proterozoic|Proterozoic|||||||07-SEP-09
24651|Albert Edward Group|23383|5|Briefly described|p20|||Ovelies the Duerdin Group.  Together with Mount House Group and Duerdin Group, correlated with Louisa Downs Group (Coates and Preiss 1980); preferred correlation with Louisa Downs Group only (Plumb 1996).||||||25-JAN-05
24651|Albert Edward Group|23599|6|Mentioned|p17|||||||||
24651|Albert Edward Group|23621|4|Described|p34|Ediacaran|Ediacaran|Overlying unit: Antrim Plateau Volcanics and King Leopold Orogeny ~560Ma. Underlying unit Duerdin Group ~600 Ma. Geological Province: Wolfe Basin.||||||02-SEP-08
24651|Albert Edward Group|23622|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Wolfe Basin.||||||
24651|Albert Edward Group|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
24651|Albert Edward Group|23821|5|Briefly described|p244|Adelaidean|Adelaidean|Geological Province: Ord Basin.||||||
24651|Albert Edward Group|24173|3|Fully described|p25, p11 Tb.2|Neoproterozoic|Neoproterozoic|Overlies Duerdin Group. Geological Province: Wolfe Basin. East of Halls Creek overlain unconformably by Antrim Plateau Volcanics (Ord Basin). Age: 650-600Ma. Correlates with Louisa Downs Group (ANGELO sheet). See also p33.||||||09-MAR-05
24651|Albert Edward Group|24503|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Siltstone, mudstone, sandstone, dolomite and conglomerate.  Geological Province: Wolfe Creek Basin.||||||
24651|Albert Edward Group|29813|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
24651|Albert Edward Group|29818|4|Described|Table 2|||||||||
24651|Albert Edward Group|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
24651|Albert Edward Group|31393|6|Mentioned|Pl.25|||Chart only||||||
24651|Albert Edward Group|32109|5|Briefly described|Table 1|||Precambrian||||||
24651|Albert Edward Group|32172|6|Mentioned|p10|||||||||
24651|Albert Edward Group|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
24651|Albert Edward Group|32660|4|Described|Table 6|||||||||
24651|Albert Edward Group|32728|6|Mentioned|Fig.3|||||||||
24651|Albert Edward Group|36532|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
24651|Albert Edward Group|36551|6|Mentioned|Table 12|||||||||
24651|Albert Edward Group|36888|4|Described|p214|||||||||
24651|Albert Edward Group|36898|6|Mentioned|p185|||See also P193.||||||
24651|Albert Edward Group|37462|4|Described|Table 4.X|||||||||
24651|Albert Edward Group|37927|6|Mentioned|p507|||||||||
24651|Albert Edward Group|38157|6|Mentioned|Table X|||||||||
24651|Albert Edward Group|38243|6|Mentioned|p357|||See also Fig.2.||||||
24651|Albert Edward Group|38988|6|Mentioned|Fig.4|||||||||
24651|Albert Edward Group|39210|5|Briefly described|p49|||||||||
24651|Albert Edward Group|41864|6|Mentioned|p15|||||||||
24651|Albert Edward Group|43299|5|Briefly described|Map Legend||Neoproterozoic|||||||
24651|Albert Edward Group|43300|5|Briefly described|Map Legend||Neoproterozoic|||||||
24651|Albert Edward Group|43301|5|Briefly described|Map Legend||Neoproterozoic|||||||
24651|Albert Edward Group|43303|5|Briefly described|Map Legend||Neoproterozoic|||||||
24651|Albert Edward Group|43595|6|Mentioned|Fig.5-34,p551|||||||||
24651|Albert Edward Group|43853|5|Briefly described|Map Legend||Proterozoic|||||||
24651|Albert Edward Group|43855|5|Briefly described|Map Legend||Proterozoic|||||||
24651|Albert Edward Group|44140|5|Briefly described|p300, p301 fig 4-7, p302 Tb.4-2|Neoproterozoic|Neoproterozoic|Osmond Range (East Kimberley) area. Associated with the 670 Ma Marinoan glaciation.|||Mount Forster, Nyuless Sandstones; Elvire, Flat Rock Formations; Boonall Dolomite; Timperley Shale.|Unconformably overlies Duerdin Group.||07-MAR-18
24651|Albert Edward Group|44155|6|Mentioned|p254 Fig.3-40|Neoproterozoic|Neoproterozoic|Sturt Block, Kimberley region.||||||
24651|Albert Edward Group|44230|5|Briefly described|Map Legend||Proterozoic|||||||
24651|Albert Edward Group|44317|14|Not recorded|p.6||Adelaidean|||||||
24651|Albert Edward Group|44318|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
24651|Albert Edward Group|44324|14|Not recorded|p.10,11||Adelaidean|(Adelaidean). Tb.2.||||||
24651|Albert Edward Group|44325|14|Not recorded|map legend||Adelaidean|||||||
24651|Albert Edward Group|44363|14|Not recorded|p.6,16,17,20|||(Adelaidean) includes Mount Forster Sandstone.||||||
24651|Albert Edward Group|44364|14|Not recorded|map legend|||||||||
24651|Albert Edward Group|44868|5|Briefly described|Map Legend||Phanerozoic|||||||
24651|Albert Edward Group|45022|14|Not recorded|p86||Adelaidean|||||||
24651|Albert Edward Group|45047|2|Defined|p194|Adelaidean|Adelaidean|Table p36.||||||23-JUL-08
24651|Albert Edward Group|45140|2|Defined|p13-14, p40, p59-60, p66, p75|||See also Appx.p35-36. Dow and Gemuts (1969). Named after Albert Edward Range. Unnamed basin NW of Birrindudu Basin. Mapped as Kearney Beds by Casey and Wells (1964). A conformable sequence of shallow-marine sediments, probably over 2000m thick. Folded and faulted.|c.650 Ma (Plumb and Derrick, 1975).||Mount Forster, Nyuless Sandstones; Elvire, Flat Rock Formations; Timperley Shale; Boonall Dolomite.|Unconformably overlies Duerdin Group. Is overlain unconformably by Antrim Plateau Volcanics and by Carranya Beds (inferred).||
24651|Albert Edward Group|46864|6|Mentioned|Fig.4|||||||||
24651|Albert Edward Group|48927|6|Mentioned|Table 1|||Refers Dow & Gemuts (1969)||||||
24651|Albert Edward Group|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Wolfe Creek Basin. Includes: Nyuless Sandstone, Timperley Shale, Boonall Dolomite, Elvire Formation, Mount Forster Sandstone.||||||
24651|Albert Edward Group|60724|5|Briefly described|p5 Fig. 2|Neoproterozoic|Neoproterozoic|||||||
24651|Albert Edward Group|63458|5|Briefly described|p872-p874; p884; p886,p897 Figs.11,19. |Ediacaran|Ediacaran|East Kimberley area.|||Includes Mount Forster Sandstone, Elvire Formation, Boonall Dolomite, Timperley Shale, Nyuless Sandstone and Flat Rock Formation.|Overlies the Duerdin Group unconformably.|Dominantly marine siliciclastics, with a relatively thin (c.40 m) carbonate unit.|
24651|Albert Edward Group|63762|5|Briefly described|p19|||Includes the Boonall Dolomite.||||||07-FEB-11
24651|Albert Edward Group|64104|6|Mentioned|p62 fig.1, p70-74, p79-80|Neoproterozoic|Neoproterozoic||||Includes Mount Forster, Nyuless Sandstones; Elvire, Flat Rock Formations; Boonall Dolomite; Timperley Shale.|Unconformably overlies Duerdin Group.||
24651|Albert Edward Group|64580|4|Described|map legend|Ediacaran|Ediacaran|Siltstone, mudstone, sandstone, dolomite and conglomerate.||||||09-DEC-08
24651|Albert Edward Group|64724|5|Briefly described|p49 Fig. 7|Ediacaran|Ediacaran|Deposited in the Wolfe Basin during the Centralian 3 event (~600-544 Ma). Shown as A.Edward Group.||||||
24651|Albert Edward Group|65413|6|Mentioned|p106 Fig.2.|||||||||
24651|Albert Edward Group|67484|6|Mentioned|p294, p295 Figs.1,2|Ediacaran|Ediacaran|East Kimberley.|||Mount Forster Sandstone, Elvire Formation, Boonall Dolomite, Timperley Shale, Nyuless Sandstone, Flat Rock Formation.|Underlain by the Duerdin Group. Overlain by the Antrim Plateau Volcanics.||
24651|Albert Edward Group|67620|5|Briefly described|p2-3, 5|Ediacaran|Ediacaran|East Kimberley region.|||Mount Forster, Nyuless Sandstones; Elvire, Flat Rock Formations; Boonall Dolomite; Timperley Shale.|Overlies Duerdin Group. Is overlain by Antrim Plateau Volcanics.||
24651|Albert Edward Group|68138|6|Mentioned|p153-154, 156|Neoproterozoic|Neoproterozoic|East Kimberley region.|||Mount Forster, Nyuless Sandstones; Elvire, Flat Rock Formations; Boonall Dolomite; Timperley Shale.|||
24651|Albert Edward Group|68244|4|Described|p659-660,666-670|Neoproterozoic|Neoproterozoic|East Kimberly area, Kimberley region. Thick marine succession comprising conformable units of sandstone and mudstone with a thin dolomite unit, the Boonall Dolomite, near the base of the group.|||Includes Flat Rock Formation, Nyuless Sandstone, Timperley Shale, Boonall Dolomite, Elvire Formation and Mount Forster Sandstone.|Overlain uncofnormably by Antrim Plateau Volcanics. Underlain unconformably by Duerdin Group.||
24651|Albert Edward Group|68473|6|Mentioned|p530-532|Neoproterozoic|Neoproterozoic|Kimberley region.|||Includes the Mt Forster Sandstone, Elvire Formation, Boonall Dolomite, Timperley Shale, Nyuless Sandstone, Flat Rock Formation.|||
24651|Albert Edward Group|68656|5|Briefly described|GEOL_LUT_CSV/500k_geologyp08_lut.csv|Ediacaran|Ediacaran|Wolfe Creek Basin, Halls Creek Orogen. See also 500k_intergeop_lut.csv|||||Undivided; siltstone, mudstone, sandstone, dolomite and conglomerate.|
24651|Albert Edward Group|69003|6|Mentioned|p5|||Halls Creek Orogen.||||||
24651|Albert Edward Group|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Wolfe Creek Basin|||Includes Flat Rock Formation, Nyuless Sandstone, Timperley Shale, Douri Sandstone, Boonall Dolomite, Elvire Formation, Mount Forster Sandstone.||Siltstone, mudstone, dolostone, and conglomerate|30-JUL-15
24651|Albert Edward Group|69165|5|Briefly described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|See also 500k_geologyp08_lut.csv.|||Includes Flat Rock Formation, Nyuless Sandstone, Timperley Shale, Douri Sandstone, Boonall Dolomite, Elvire Formation, Mount Forster Sandstone.||Undivided; siltstone, mudstone, dolostone and conglomerate.|
24651|Albert Edward Group|69437|6|Mentioned|p22:4-5|||Wolfe Basin.|||Mount Forster Sandstone.|||12-JUL-16
24651|Albert Edward Group|69442|6|Mentioned|p27:1, 6|||Wolfe Basin.|||Mount Forster Sandstone.|||12-JUL-16
24651|Albert Edward Group|69445|5|Briefly described|p30:4, 16-17|||Dow and Gemuts (1967). Eastern Kimberley region.|||Mount Forster Sandstone.|Is overlain unconformably by Antrim Plateau Volcanics.||12-JUL-16
24651|Albert Edward Group|69587|4|Described|GEOL_LUT_CSV files|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen, North Australian Craton. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1. See 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|635-541 Ma (inferred)||||Siltstone, mudstone, dolostone, and conglomerate|
24651|Albert Edward Group|69597|6|Mentioned|p5 fig 2b|||||||||
24651|Albert Edward Group|69634|4|Described|GEOL_LUT_CSV files|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|635-541 Ma (inferred)||Includes Boonall Dolomite, Douri Sandstone, Elvire Formation, Flat Rock Formation, Mount Forster Sandstone, Nyuless Sandstone, Timperley Shale.||Undivided; siltstone, mudstone, sandstone, dolomite and conglomerate|
24651|Albert Edward Group|70154|6|Mentioned|100k_interpgeop_lut.csv|||See also 500k_interpgeop_lut.csv.|||Includes Flat Rock Formation, Nyuless Sandstone, Timperley Shale, Douri Sandstone, Boonall Dolomite, Elvire Formation, Mount Forster Sandstone.|||
24651|Albert Edward Group|70731|5|Briefly described|p268|Neoproterozoic|Neoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.||||Equvalent to Mount House Group.||
24651|Albert Edward Group|70826|6|Mentioned|p5 tbl 2|||Supersequence 3 and 4, Centralian Superbasin.||||||20-APR-20
24651|Albert Edward Group|70851|6|Mentioned|p18-p19|||||||||
24651|Albert Edward Group|71146|5|Briefly described|p6, p21|Cambrian|Cambrian|Bonaparte Basin. Age is tentative. ||||Overlies the Boonall Dolomite. Unconformably overlain by the Antrim Plateau Volcanics.|Mixed sandstone, mudstone and coal.|
24651|Albert Edward Group|71267|4|Described|GEOL_LUT_CSV files|||Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyl12_lut.csv.|||Includes Boonall Dolomite, Douri Sandstone, Elvire Formation, Flat Rock Formation, Mount Forster Sandstone, Nyuless Sandstone, Timperley Shale.||Fine- to medium-grained quartz sandstone; minor pebbly sandstone and conglomerate|
24651|Albert Edward Group|72034|5|Briefly described|500k_interpgeop16_lut|Ediacaran|Ediacaran|Wolfe Basin.|||||Siltstone, mudstone, dolostone, and conglomerate.|
24651|Albert Edward Group|73255|6|Mentioned|p534 Fig.2|Ediacaran|Ediacaran|[Misspelt as Edward Albert Group on p535?]|||Mount Forster Sandstone, Elvire Formation, Boonall Dolomite, Timperley Shale, Nyuless Sandstone, Flat Rock Sandstone.|Overlies the Ranford Formation, Duerdin Group.||
39599|Alcurra Dolerite|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Dolerite dykes. Geological Province: Musgrave Block.||||||
39599|Alcurra Dolerite|61154|2|Defined|p42 App., p13, p15-16, p44|Mesoproterozoic|Mesoproterozoic|Dolerite with ophitic to subophitic texture contains plagioclase. Unconformable over Dean Quartzite. Intrudes Pitjantjatjara Supersuite (Kugera Gr. and Ayers Range Gr). Intruded by Angatja Granite. Age: 1080Ma. Geol.Prov: Musgrave Block.||||||01-SEP-09
39599|Alcurra Dolerite|61524|5|Briefly described|p16|||Mafic dykes associated with the Giles Complex. Geological Province: Musgrave Province.||||||
39599|Alcurra Dolerite|61733|5|Briefly described|p46, p56|||Musgrave Block. Has subduction-related isotopic and geochemical signatures. Emplaced during the Warakurna igneous event at c.1.08-1.05 Ga.|c.1.08 Ga.||||High-Mg, low-Ti tholeiites.|
39599|Alcurra Dolerite|64722|6|Mentioned|p17|Stenian|Stenian|Of a similar age to granites dated at 1080-1070 Ma.|||||Mafic tholeiitic dykes.|11-APR-12
39599|Alcurra Dolerite|64745|5|Briefly described|p376|Stenian|Stenian|Dykes. Age: ca. 1.08 Ga (Sm-Nd isochron Plag-Opx-Cpx. Zhao and McCulloch, 1993). May represent feeder system to Giles Intrusions. Geol. Prov: Musgrave Province.||||||
39599|Alcurra Dolerite|65135|6|Mentioned|p17|Stenian|Stenian|~1070 Ma. Shows geochemical similarities to Giles Event intrusives and the Warakurna Large Igneous Province.||||||
39599|Alcurra Dolerite|65369|5|Briefly described|p35|||Central Australian intraplate (flood-type) basalt.||||||19-MAR-12
39599|Alcurra Dolerite|65693|4|Described|p4,p7- p8 Fig.5, p9-12 Figs. 8-10.|||See also Alcurra Suite, Alcurra suite. Geochemistry is different from Tollu Group: detailed in text. Ages are Ar/Ar from Schmidt et al. (2006).|1085 +/- 2 to 1068 +/- 2 Ma|Unit in Alcurra Suite.|||Relatively evolved, Fe-rich, incompatible trace element-rich suite of tholeiitic intrusions.|22-APR-20
39599|Alcurra Dolerite|65833|5|Briefly described|p17|Stenian|Stenian|Formed during ~1075 Ma Giles Event. Intrudes Pitjantjatjara Supersuite.||||||
39599|Alcurra Dolerite|65906|6|Mentioned|p7|Mesoproterozoic|Mesoproterozoic|~1070 Ma.||||||
39599|Alcurra Dolerite|67128|6|Mentioned|p6|||||Warakurna Supersuite.|||Mafic dykes.|
39599|Alcurra Dolerite|67244|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||c.1067 Ma.|Unit in Warakurna Supersuite.|||Dykes, sills or plugs mainly of dolerite; also of olivine gabbro, accessory biotite, massive to weakly flow-banded; and fine- to medium-grained plagioclase-phyric gabbro, ophitic texture, plagioclase phenocrysts and glomerophenocrysts to 2 cm.|11-APR-12
39599|Alcurra Dolerite|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||c.1068 Ma.|Unit in Warakurna Supersuite.|||Dykes, sills or plugs mainly of dolerite and metadolerite but also of olivine gabbro, olivine norite, ferronorite, and ferrodiorite.|
39599|Alcurra Dolerite|67375|4|Described|p13, p19 Fig.11, pp36-37, p41, pp332-339|Mesoproterozoic|Mesoproterozoic|A suite of rocks including the Alcurra Dolerite dyke swarm, small intrusions emplaced peripheral to the Warakurna Supersuite, and the compositionally equivalent olivine-rich gabbros, olivine norites, ferronorites and ferrodiorites which host the Nebo-Babel nickel-copper-PGE sulfide mineralization.|1068 +/- 7 - 1067 +/- 8 Ma (Kirkland et al. 2009).|Unit in Warakurna Supersuite.||Intrudes the Smoke Hill Volcanics and Giles Suite.|Dykes, sills and plugs mainly of dolerite but also of olivine gabbros, olivine norites, ferronorites and ferrodiorites.|
39599|Alcurra Dolerite|67553|5|Briefly described|p11,20,34,37-41,p65, 89,95|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Makes up the Warakurna Supersuite component within the Walpa Pulka Zone. Intrusive age from GSWA 194354, coeval with emplacement of Smoke Hill Volcanics. Highly evolved iron-rich tholeiitic intrusions intruding at a relatively late stage in the Giles Event at c. 1067 Ma. At least locally, these rocks are directly related to orthomagmatic nickel-copper mineralization (Howard et al., 2009).|1068+\-7 Ma|Unit of Warakurna Supersuite.||||06-AUG-19
39599|Alcurra Dolerite|68995|6|Mentioned|p1, p8, p50-56, p61, p64-65.|Mesoproterozoic|Mesoproterozoic|Referred to on p1 as the informal Alcurra Dolerite dyke swarm. Intruded during the Mesoproterozoic Giles Event. Source and origin of this unit is discussed in great detail.||||||
39599|Alcurra Dolerite|68996|5|Briefly described|p7, 24-25, 28-29, 32,33, 35-46,53,54,66|Mesoproterozoic|Mesoproterozoic|Hosts significant mineralization of the Nebo-Babel Ni-Cu-PGE deposit. Includes Saturn gabbro. Age range from current dating may not recognise prolonged magmatism suggested from field relationships. See also Alcurra Dolerite Suite p9.|1072-1068 Ma magmatic||Includes Saturn gabbro.||Dolerite dykes and sills. Average density of 2.98+/-0.17g/cm^3|
39599|Alcurra Dolerite|69003|5|Briefly described|p50|Mesoproterozoic|Mesoproterozoic|Associated with the Giles Event. Hosts the orthomagmatic Ni-Cu-PGE mineralisation of the Nebo-Babel deposit, described in some detail on p51.|c.1070 Ma.||||Iron-rich tholeiitic mafic dykes and sills.|
39599|Alcurra Dolerite|69009|5|Briefly described|Map Legend|Stenian|Stenian||c. 1068 Ma|Of the Warakurna Supersuite.|||Comprises dykes, sills, or plugs, with olivine gabbro, olivine norite, ferronorite, and ferrodiorite.|
39599|Alcurra Dolerite|69091|4|Described|p54 Fig.4.2, p74, p103 Fig.5.6|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province (Wingate et al., 2004). Hogarth Formation is compositionally identical with an identical crystallisation age of 1068 +/- 7 Ma. Appears as Alcurra Dolerite Suite on p132, p134 Fig.6.2, p137-138, p141 Fig.6.8, p144, p204-205.|1068 +/- 7 Ma|Warakurna Supersuite|Saturn gabbro||Mafic intrusions; most are relatively small dykes and sills, however some larger intrusions exist.|
39599|Alcurra Dolerite|69153|5|Briefly described|GEOL_LUT_CSV files;GEOCHRON/194354.1.pdf|Mesoproterozoic|Mesoproterozoic|Geochron analysis (194354) of medium- to coarse-grained, ophitic gabbro dyke. 20 analyses|1067+/-8 Ma SHRIMP-A|Warakurna Supersuite|||Dolerite in dykes, sills, or plugs, with olivine gabbro, olivine norite, mesocratic orthopyroxene(-olivine) ferronorite to ferrodiorite|
39599|Alcurra Dolerite|69427|6|Mentioned|p12:46|||Musgrave Province.||||Is correlated with Stuart Pass Dolerite (Aileron Province).||12-JUL-16
39599|Alcurra Dolerite|69428|6|Mentioned|p13:16|||Musgrave Province.||||Correlated with the Stuart Pass Dolerite.||12-JUL-16
39599|Alcurra Dolerite|69436|4|Described|p21:1, 4, 11-14, 20-21|Mesoproterozoic|Mesoproterozoic|Edgoose et al. (1993). Widespread throughout Musgrave Province. Related to the Giles Event (1085-1040 Ma). Chilled margins on some dykes suggest shallow-level intrusions. Similar geochemistry to Mount Harris Basalt suggests a common source. As potential feeders for the Giles Complex, some larger dykes have potential for Cu-Ni-Co mineralisation. Geochronology by Camacho et al. (1991) and Zhao and McCulloch (1993) respectively.|1054 +/- 14 Ma (Rb-Sr); 1090 +/- 32 Ma (Sm-Nd).|Warakurna Supersuite.||Intrudes Musgravian gneiss and Pitjantjatjara Supersuite. Is intruded by Angatja Suite.|Extensive intrusions of dolerite and subordinate gabbro dykes, typically 1-3m wide, but up to 8m wide and 6km long. Geochemically homogeneous olivine tholeiite, generally ophitic to sub-ophitic. Locally metamorphosed to garnet granulite facies.|12-JUL-16
39599|Alcurra Dolerite|69437|6|Mentioned|p22:11-12|||Associated with the c.1070 Ma Warakurna Large Igneous Province. Emplaced within the Musgrave Province.||||||12-JUL-16
39599|Alcurra Dolerite|69438|6|Mentioned|p23:9|||Intrudes basement rocks of the Aileron Province.||||||12-JUL-16
39599|Alcurra Dolerite|69640|6|Mentioned|p11|Proterozoic|Proterozoic|Musgrave Province.||||Intrudes the Pitjantjatjara Supersuite.||
39599|Alcurra Dolerite|69655|6|Mentioned|p58|||||||||
39599|Alcurra Dolerite|69729|5|Briefly described|p68, p74 Fig.8, p80-84, p86|Mesoproterozoic|Mesoproterozoic|Edgoose et al. (1993); Scrimgeour et al. (1999). Warakurna Large Igneous Province. Originally defined from the Kulgera region (NT). Geochemistry and provenance discussed; trace element plot.|c.1078 Ma to 1073 Ma.|||Is cross-cut by Kullal Dyle Suite.||
39599|Alcurra Dolerite|70083|6|Mentioned|p207|||Musgrave Inlier. Associated with the Giles Event.|~1085-1050 Ma.|Giles Complex.||Intrudes Birksgate Complex.||
39599|Alcurra Dolerite|70338|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Dolerite, dark grey, medium- to fine-grained, olivine, hypersthene. Poikilitic texture.|
39599|Alcurra Dolerite|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|SHRIMP age from dolerite (19454.1.pdf)|1067 Ma - 1068 Ma (Isotopic) 1067  (SHRIMP)|Warakurna Supersuite|||Dolerite dykes, sills or plugs with olivine gabbro, olivine norite, ferronorite and ferrodiorite. Fine-medium grained plagioclase-phyric dolerite and gabbro. Olivine rich gabbro, fine-grained, mesocratic ferronorite to ferrodiorite.|
39599|Alcurra Dolerite|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province. Of Warakurna Large Igneous Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Warakurna Supersuite Magmatic Event (1084-1040 Ma); Giles Event (1085-1040 Ma). Sample GSWA 194354 (gabbro dyke) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) magmatic crystallisation age of 1067+\-8 Ma. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv.|1068-1067 Ma (inferred)|Unit of Warakurna Supersuite.|||Dolerite in dykes, sills, or plugs, with olivine gabbro, olivine norite, ferronorite, and ferrodiorite; mesocratic pox-olivine ferronorite to ferrodiorite.|
39599|Alcurra Dolerite|70826|6|Mentioned|p10, p14 tbl 5|Mesoproterozoic|Mesoproterozoic|Musgrave Province. |1068-1067 Ma|Warakurna Supersuite.||||20-MAY-20
39599|Alcurra Dolerite|70831|5|Briefly described|p4-p5|Stenian|Stenian|Musgrave Province.|c. 1085-1040 Ma|Warakurna Supersuite||||
39599|Alcurra Dolerite|71170|5|Briefly described|p6|||||||||
39599|Alcurra Dolerite|71210|5|Briefly described|p5, p10-p12, p15, p20, p43,|Stenian|Stenian|Musgrave Province. C. 1080 Ma age is derived from Edgoose et al., 1993; Scrimgeour et al., 1999 and Howard et al., 2009c. Hosts most of the magmatic sulphide mineralisation of the Musgrave Province, including the Nebo-Babel Ni-Cu-PGE deposit. Previously referred to as the G3 member of the Giles Suite. See also p46, p50, p66-p67, p69, p76, p109, p114, p134, p139.|c. 1080 Ma -1068 Ma||||Dolerite, olivine gabbros, norites, ferronorites and diorites.|
39599|Alcurra Dolerite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolerite|
39599|Alcurra Dolerite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Of Warakurna Large Igneous Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Warakurna Supersuite Magmatic Event (1084-1040 Ma); Giles Event (1085-1040 Ma). Sample GSWA 194354 (gabbro dyke) yielded a weight mean 207Pb/206Pb age of 1067+\-8 Ma, interpreted as magmatic crystallisation age. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv.|1068+\-4 Ma; 1067+\-8 Ma|Unit of Warakurna Supersuite.|||Dolerite dykes and plugs; plagioclase-phyric dolerite and gabbro; ferronorite: mesocratic opx-olivine, magnetite-rich; mesocratic opx ferrnonorite to ferrodiorite.|
39599|Alcurra Dolerite|71321|6|Mentioned|p1,11,23, 50,58,64|Stenian|Stenian|Geological province: Musgrave Province. Comprises part of basement to the Musgrave Province i.e. intrudes and cross-cuts Musgravian-aged gneisses and granites. Associated with c. 1080 Ma Giles Event (p11 for references).||||||24-OCT-19
39599|Alcurra Dolerite|71416|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province. Interpreted age from correlation with Giles Complex.|~1080 Ma.|Warakurna Supersuite.||Correlated with Giles Supersuite.|Massive olivine dolerite, mainly E-trending dykes.|
39599|Alcurra Dolerite|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1067+/-8 Ma (crystallisation: U-Pb zircon SHRIMP)||||Gabbro with ophitic texture and interstitial pyroxene.|
39599|Alcurra Dolerite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic||Max age 1068+/-4, min 1067+/-8 Ma.|Warakurna Supersuite|||Dolerite in dykes, sills, or plugs, with olivine gabbro, olivine norite, ferronorite, and ferrodiorite.|
39599|Alcurra Dolerite|72094|6|Mentioned|p2, p3 Fig 2|Mesoproterozoic|Mesoproterozoic|Musgrave Province.||Unit of Warakurna Supersuite.||||
39599|Alcurra Dolerite|72238|5|Briefly described|p34-36,38-42|Stenian|Stenian|Geological province: Musgrave Province. Dimensions: mainly <10m, rarely up to 80m wide. Associated with coeval Giles Complex mafic-ultramafic intrusions (prospective for orthomagmatic Ni-Cu PGE mineralisation (Howard et al. 2009). Forms part of the Warakurna Large Igneous Province (Wingate, Pirajno and Morris 2004). Generally of lower olivine content than Amata Dolerite. Locally crosscut by Amata Dolerite dykes. Commonly shows evidence for contamination by host rocks. Sm-Nd isochron age: 1110+\-56 Ma.|c. 1080 Ma|||||
39599|Alcurra Dolerite|72443|5|Briefly described|p737, 739, p748, p751-752, p757|||Emplaced over much of central and western Australia and represents much of the Warakurna Large Igneous Province.|1078-1073 Ma|Warakurna Supersuite|||Dolerite dykes and sills.|
39599|Alcurra Dolerite|72476|6|Mentioned|p35, 39|||Musgrave Province. Intrusion of these sills and dykes is suggested to have reset the apatite U-Pb clock in the easternmost parts of the Province. Associated with the mafic/ultramafic Warakurna Large Igneous Province. See also reference to Alcurra Dolerites (p25).||||||
39599|Alcurra Dolerite|73232|6|Mentioned|p5|||Musgrave Province. [Emplaced] during the Giles Event. Includes dykes.||Giles Complex||Intrudes Birksgate Complex and Pitjantjatjara Supersuite.||
39599|Alcurra Dolerite|73437|6|Mentioned|p151|Mesoproterozoic|Mesoproterozoic|||Warakurna Supersuite||||
25758|Alexander Formation|7433|4|Described|p25 Fig.2, p43. |Kimmeridgian|Oxfordian|Canning Basin. Shallow marine, largely tidal, clastics.||||Overlies Wallal Sandstone. Is overlain by Jarlemai Siltstone and probably Frezier Sandstone.|Sandstone; numerous mudstone interbeds; minor conglomerate. Cross-bedding, ripples, flaser bedding, shelly fossils and bioturbation common.|
25758|Alexander Formation|22718|5|Briefly described|P8, Table1 P6||Oxfordian|||||||
25758|Alexander Formation|22738|4|Described|10,13,16, map|Late Jurassic|Late Jurassic|Max thickness: 60m. Overlain by Jarlemai Siltstone, underlain by Wallal Sandstone.||||||13-NOV-07
25758|Alexander Formation|22741|5|Briefly described|P30, Table3 P11|Tithonian|Kimmeridgian|||||||
25758|Alexander Formation|22753|5|Briefly described|Fig.3 p585|Jurassic|Jurassic|||||||
25758|Alexander Formation|22765|5|Briefly described|P10, Table1|Kimmeridgian|Oxfordian|||||||
25758|Alexander Formation|22767|5|Briefly described|Table3 P12, P23||Late Jurassic|||||||
25758|Alexander Formation|22776|4|Described|Table.3|Late Jurassic|Late Jurassic|||||||
25758|Alexander Formation|22801|5|Briefly described|P12, Table1 P8|Kimmeridgian|Late Oxfordian|||||||
25758|Alexander Formation|22814|5|Briefly described|fig2|Jurassic|Jurassic|||||||
25758|Alexander Formation|23212|4|Described|Table.1 p11||Oxfordian|Dated by rich macrofauna to be Late Jurassic (Oxfordian).||||||
25758|Alexander Formation|23722|6|Mentioned|p35|||||||||
25758|Alexander Formation|23765|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||
25758|Alexander Formation|23766|4|Described|p13 Tb. 2|Late Jurassic|Early Jurassic|Comprises sandstone, siltstone and minor conglomerate.  Thickness: 219m.  See also p26.||||||13-NOV-07
25758|Alexander Formation|24061|5|Briefly described|p183|Jurassic|Jurassic|Geological Province:  Canning Basin.||||||
25758|Alexander Formation|24062|5|Briefly described|p186 Table 1|Jurassic|Jurassic|Geological Province: Canning Basin.||||||
25758|Alexander Formation|24449|5|Briefly described|p741 Fig. 2|Oxfordian|Oxfordian|Age: ~150m.y.  Geological Province: Canning Basin.||||||
25758|Alexander Formation|30110|6|Mentioned|p81|||See also p84. Middle Jurassic, Kimmeridgian.||||||10-FEB-20
25758|Alexander Formation|30313|5|Briefly described|p54|||Jurassic age||||||
25758|Alexander Formation|30897|6|Mentioned|p19|||Subsurface unit||||||
25758|Alexander Formation|31153|6|Mentioned|p111|||Refers Bivalves of Canning Basin||||||
25758|Alexander Formation|31396|6|Mentioned|p1184|||||||||
25758|Alexander Formation|32648|6|Mentioned|p32|||U.Jur.||||||
25758|Alexander Formation|32979|6|Mentioned|p38|||Correlation with basins in India||||||
25758|Alexander Formation|33166|6|Mentioned|p67|||Stratigraphy||||||
25758|Alexander Formation|34134|6|Mentioned|p482|||Upper Jurassic||||||
25758|Alexander Formation|34363|6|Mentioned|p56|||See Fig.7. Kimmeridgian.||||||
25758|Alexander Formation|35275|6|Mentioned|Fig.5.|||||||||
25758|Alexander Formation|35711|6|Mentioned|Table 4|||||||||
25758|Alexander Formation|35969|6|Mentioned|Table 7|||||||||
25758|Alexander Formation|36224|5|Briefly described|Map legend|Late Jurassic|Late Jurassic|Fine to medium sandstone, interbedded mudstone; bioturbated; minor conglomerate lenses; fossiliferous.||||||01-FEB-05
25758|Alexander Formation|36225|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
25758|Alexander Formation|36257|6|Mentioned|Table 2.1|||||||||
25758|Alexander Formation|36438|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
25758|Alexander Formation|36634|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
25758|Alexander Formation|36890|3|Fully described|p347|||||||||
25758|Alexander Formation|37364|6|Mentioned|p1051|||||||||
25758|Alexander Formation|37368|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
25758|Alexander Formation|37369|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
25758|Alexander Formation|37370|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
25758|Alexander Formation|38444|6|Mentioned|p301|||||||||
25758|Alexander Formation|38878|6|Mentioned|Map legend|Kimmeridgian|Oxfordian|Oxfordian - Kimmeridgian||||||
25758|Alexander Formation|38886|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
25758|Alexander Formation|39857|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
25758|Alexander Formation|40045|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
25758|Alexander Formation|40078|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
25758|Alexander Formation|40992|6|Mentioned|Fig.11|||||||||
25758|Alexander Formation|41169|6|Mentioned|Fig.3|||||||||
25758|Alexander Formation|41436|6|Mentioned|p46|||||||||
25758|Alexander Formation|41639|6|Mentioned|p14|||||||||
25758|Alexander Formation|41730|6|Mentioned|Fig.3|||||||||
25758|Alexander Formation|42338|5|Briefly described|Table 1 P145|||||||||
25758|Alexander Formation|42571|4|Described|p17|||||||||
25758|Alexander Formation|42572|5|Briefly described|Map Legend|Jurassic||||||||
25758|Alexander Formation|42734|5|Briefly described|map legend|Jurassic||||||||
25758|Alexander Formation|42792|5|Briefly described|Table 1 P225|||||||||
25758|Alexander Formation|42814|5|Briefly described|p24|||||||||
25758|Alexander Formation|42930|5|Briefly described|Fig.1 p473|Late Jurassic|Late Jurassic|Unconformably overlies Wallal and Barbwire Sandstones; conformably overlain by Jarlemai Siltstone. Geological Province: Canning Basin.||||||24-NOV-08
25758|Alexander Formation|43563|6|Mentioned|Fig.2,p5||Late Jurassic|||||||
25758|Alexander Formation|43656|6|Mentioned|Fig.2,p8|Kimmeridgian|Oxfordian|||||||
25758|Alexander Formation|43666|6|Mentioned|p45,Table 2||Kimmeridgian|||||||
25758|Alexander Formation|43746|6|Mentioned|Fig.2,p11|Kimmeridgian|Oxfordian|||||||
25758|Alexander Formation|43818|6|Mentioned|Fig.2.p39||Late Jurassic|||||||
25758|Alexander Formation|44040|14|Not recorded|p43|||||||||
25758|Alexander Formation|44143|4|Described|p.433 Table 4-19; p.449|Jurassic|Jurassic|Up to 92m thick; fine to medium sandstone, interbedded with mudstone. Conformably overlies Wallal Sandstone. Shallow marine; type section at Mt Alexander (MOUNT ANDERSON: 18deg 41'  00" S, 123deg 39' 20" E).||||||22-NOV-17
25758|Alexander Formation|44357|4|Described|p13,Tb.1 p9||Late Jurassic|Subsurface only.||||||
25758|Alexander Formation|44403|2|Defined|p.6, Table 1|||Less than 180 ft. fossils: ammonites and pelecypods of Lower Portlandian or Kimmeridgian age. Lithology similar to above. E/51-12.||||||
25758|Alexander Formation|44404|14|Not recorded|map legend||Jurassic|||||||
25758|Alexander Formation|44997|14|Not recorded|p.36,39|||||||||
25758|Alexander Formation|44998|2|Defined|p148|||Overlies Jurgurra Formation. p119,131-2,-5-6,143-151,-4,-7,185,-8,246. See also App.4 p283.||||||
25758|Alexander Formation|45153|2|Defined|App.6-97|Oxfordian|Oxfordian|Previously included in Fraser River beds.||||||13-NOV-07
25758|Alexander Formation|45158|3|Fully described|p16|||||||||
25758|Alexander Formation|45168|6|Mentioned|p6|||||||||
25758|Alexander Formation|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
25758|Alexander Formation|48596|14|Not recorded|p.5|||(E51-11)||||||
25758|Alexander Formation|48837|14|Not recorded|p.6,10,13|||?Mr Anderson E/51-11.||||||
25758|Alexander Formation|61021|5|Briefly described|p36 Fig. 2|Kimmeridgian|Oxfordian|Geological Province: Canning Basin.||||||17-DEC-07
25758|Alexander Formation|64186|5|Briefly described|p171, p170 Fig. 1|Oxfordian|Oxfordian|Underlain by Wallal Sandstone, overlain by Jarlemai Siltstone. Max thickness: 60m.||||||
25758|Alexander Formation|64580|4|Described|map legend||Late Jurassic|Fine- to medium-grained sandstone, mudstone.||||||09-DEC-08
25758|Alexander Formation|64643|5|Briefly described|p3 Fig. 2|Late Jurassic|Late Jurassic|||||||10-FEB-20
25758|Alexander Formation|64982|6|Mentioned|p700.|||||||||
25758|Alexander Formation|65301|5|Briefly described|p5 Fig. 4|Late Jurassic|Late Jurassic|Geological province: Canning Basin.||||||
25758|Alexander Formation|65449|5|Briefly described|p6|Late Jurassic|Late Jurassic|||||Overlies Wallal and Barbwire Sandstones. Is overlain by Jarlemai Siltstone.||
25758|Alexander Formation|67202|5|Briefly described|p69-71|Late Jurassic|Late Jurassic|20-92m thick. Shallow-marine to tidal deposits.|||||Sandstone interbedded with mudstone, cross-bedded, ripple-marked, minor conglomerate.|
25758|Alexander Formation|68007|6|Mentioned|p4, p8|Late Jurassic|Late Jurassic|Canning Basin. Interpreted as 23.5m thick in Patience 1 well (222-245.5m depth), Menzel and Lipski (1986). No biostratigraphic data presented.||||||19-FEB-20
25758|Alexander Formation|68811|6|Mentioned|p79|Jurassic|Jurassic|Seawater intrusion has been measured within this units aquifer. ||||||
25758|Alexander Formation|68902|6|Mentioned|p9 fig 5|Jurassic|Jurassic|||||Overlies Wallal and Barbwire Sandstones. Is overlain by Jarlemai Siltstone.||
25758|Alexander Formation|69029|6|Mentioned|p319|Kimmeridgian|Oxfordian|Of Canning Basin.||||Overlain by Jarlemai Siltstone. Underlain by Wallal Sandstone.||
25758|Alexander Formation|69182|6|Mentioned|Ch4 p3, Ch4 p9|Late Jurassic|Late Jurassic|Canning Basin. See also Ch4 p30-p35, Ch4 p45, Ch4 p83-p84. ||||Overlies the Wallal and Barbwire Sandstones. Overlain by the Jarlemai Formation.||10-FEB-20
25758|Alexander Formation|69297|6|Mentioned|p337, p352|Tithonian|Kimmeridgian|Broome Platform of the Canning Basin. ||||Overlies the Barbwire Sandstone. Overlain by the Jarlemai Siltstone.||
25758|Alexander Formation|69312|5|Briefly described|p3|Kimmeridgian|Oxfordian|Canning Basin. ||||Overlies the Wallal Sandstone. Overlain by the Jarlemai Siltstone.|Sandstone with minor carbonate interbeds.|
25758|Alexander Formation|70774|5|Briefly described|p4|Late Jurassic|Late Jurassic|Canning Basin.||||Overlies the Wallal and Barbwire Sandstones. Overlain by the Jarlemai Siltstone.||10-FEB-20
25758|Alexander Formation|70826|6|Mentioned|p7 tbl 4|Early Cretaceous|Jurassic|Canning Basin.||||||
25758|Alexander Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||mudstone, conglomerate, sandstone|
25758|Alexander Formation|71894|5|Briefly described|p4|Late Jurassic|Late Jurassic|Canning Basin.||||Overlies the Barbwire Sandstone and the Wallal Sandstone. Overlain by the Jarlemai Formation.|Sandstone, shale and conglomerate.|10-FEB-20
25758|Alexander Formation|72034|5|Briefly described|500k_interpgeop16_lut|Kimmeridgian|Oxfordian|Canning Basin.  Age from biostratigraphy.|||||Fine- to medium-grained sandstone, mudstone.|
25758|Alexander Formation|72497|5|Briefly described|p3 Fig.2.|Kimmeridgian|Callovian|Shown as occuring in the Anketell, Tabletop, Ryan Shelves, Willara and Kidson Sub-basins, the Jurgurra and Barbwire Terraces and Broome Platform. Also shown as occuring in the  Fitzroy Trough, Betty and Balgo Terraces and part of the Lennard Shelf and Margaret Terrace.||||Conformably overlies Wallal Sandstone. Conformably underlies Jarlemai Siltstone. Laterally equivalent in part to Barbwire and Meda Sandstones.||
25758|Alexander Formation|72499|4|Described|p7, p10, p53, p84, p89, p91.|Late Jurassic|Late Jurassic|Located in the Willara Sub-basin, Broome Platform and the Fitzoy Trough. Identified in Dampier Downs 1, Perindi 1, Roebuck Bay 1 well logs. Ref Forman and Wales, 1981. Fluvio-deltaic setting.||||Overlies Wallal and Barbwire Sandstones|Dominantly sandstone and some shale. Conglomerate at base.|
25758|Alexander Formation|73117|5|Briefly described|p3|Upper Jurassic|Upper Jurassic|Canning Basin.||||Underlain by Wallal Sandstone and Barbwire Sandstone. Overlain by Jarlemai Siltstone.|Dominantly sandstone with lesser shale and conglomerate in the lower portion in the north[?].|
39341|Alicia Granite|24091|4|Described|p35|Archean|Archean|LEONORA 1:250 000, WEEBO 1:100 000. Age: 2693+/-3Ma (Pb/Pb). Geological Province: Yilgarn Craton.||||||07-NOV-08
23326|Allanson Sandstone|14227|5|Briefly described|Enclos. 2|Artinskian|Artinskian|Overlies Ewington Coal Measures; underlies Premier Coal Measures. Presented as Allanson SST.||||||07-FEB-11
23326|Allanson Sandstone|22820|5|Briefly described|p10 Fig.4|Late Permian|Early Permian|Of the Collie Group.||||||11-AUG-08
23326|Allanson Sandstone|23174|5|Briefly described|Fig5p8|||||||||
23326|Allanson Sandstone|42711|5|Briefly described|p4 Fig. 3, p24-25,  Plates 2, 4, 5|Early Permian|Early Permian|Of Collie Group. Conformable over Ewington C.M.; conformable below Premier C.M. Geological province: Collie Basin. Poorly sorted feldspathic sandstone, subordinate conglomerate, siltstone, carbonaceous shale and sporadic coal. Lith. details given.||||||11-AUG-08
23326|Allanson Sandstone|43442|6|Mentioned|p50|||||||||
23326|Allanson Sandstone|64580|5|Briefly described|map legend|||Of Collie Group. Sandstone with interbedded subordinate siltstone in coarsening-upward sequence.||||||15-DEC-08
23326|Allanson Sandstone|70097|5|Briefly described|p19 Fig.3|Kungurian|Kungurian|Southern Perth Basin. Collie Sub-basin.||Collie Group||Overlies Ewington Coal Measures. Is overlain by Premier Coal Measures.|Sandstone.|30-SEP-16
23326|Allanson Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Artinskian|Artinskian|Perth Basin.  Age from biostratigraphy.||Collie Group.|||Poorly sorted feldspathic sandstone; lesser pebble conglomerate, siltstone, carbonaceous; local coal.|
34450|Amhurst Metamorphics|23383|3|Fully described|p16, p5 Tb. 1|Paleoproterozoic|Paleoproterozoic|In the Lamboo Complex. Formed by metamorphism of Marboo Formation and Neville Granodiorite (Sally Downs supersuite intrusions); paragneiss and orthogneiss.  Age: 1835-1805Ma. Geological Province: Halls Creek Orogen.  See also p6 Fig. 3.||||||07-NOV-08
34450|Amhurst Metamorphics|23601|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
34450|Amhurst Metamorphics|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: <1865-1850Ma.||||||07-NOV-08
34450|Amhurst Metamorphics|44694|5|Briefly described|Map Legend||Proterozoic|||||||
34450|Amhurst Metamorphics|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.|||Divided into igneous and metasedimentary gneisses.||biotite-hornblende granodiorite gneiss, and biotite-andalusite-garnet-cordierite monzogranitic gneiss; inclusions of metasedimentary and mafic meta-igneous rock|
34450|Amhurst Metamorphics|69165|4|Described|500k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|alternate spelling of amherst metamorphics.|||||granitic gneiss and metasedimentary rock.|15-DEC-22
34450|Amhurst Metamorphics|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|1872-1860 Ma (Inferred)|||May be equivalent to Neville Granodiorite or Marboo Formation.|Granodiorite gneiss, monzogranitic gneiss; inclusions of metasedimentary and mafic meta-igneous rock,  schist, granofels, and migmatite.|
34450|Amhurst Metamorphics|70154|5|Briefly described|500k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1860-1872 Ma||||Granitic gneiss and metasedimentary rock|
34450|Amhurst Metamorphics|70812|5|Briefly described|p3, p10, p18-p19, p27, p30|||Mineralisation is described.||||In part equivalent to the Marboo Formation.||
34450|Amhurst Metamorphics|71140|6|Mentioned|p99 Tb.1|||Western Zone, Lamboo Province, Halls Creek Orogen. High-grade metamorphics. Representative mineral assemblage listed.||||||
34450|Amhurst Metamorphics|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (183 -1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). Metamorphosed equivalent of Marboo Formation. See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|1872-1860 Ma (inferred)||||Biotite-hornblende granodiorite gneiss, and biotite-andalusite-garnet-cordierite monzogranitic gneiss; inclusions of metasedimentary and mafic meta-igneous rock, granofels, and migmatite|
34450|Amhurst Metamorphics|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Central Zone, Halls Creek Orogen.|||||Granitic gneiss and metasedimentary rock.|
34450|Amhurst Metamorphics|72437|6|Mentioned|p13|||Interpreted by Griffin and Tyler (in prep.) as Marboo Formation and c. 1860 Ma Neville Granodiorite. Three analyses of the orthogneisses are presented.||||Intruded by the Sally Downs supersuite.|Mixture of high-grade paragneisses and orthogneisses.|
35317|Amputjuta Dacite|50321|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Pottoyu Granite Suite.  Geological Province: Musgrave Block.  Age: ~1150Ma.||||||09-JUN-04
35317|Amputjuta Dacite|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Pitjantjatjara Supersuite.  Finely porphyritic hypabyssal dacite.  Geological Province: Musgrave Block.||||||12-JAN-05
35317|Amputjuta Dacite|61154|5|Briefly described|p10, p44 App., p28|Mesoproterozoic|Mesoproterozoic|Of Pottoyu Suite (Pitjanjatjara Supersuite). A hybabyssal intrusive unit containing phenocrysts of plagioclase and qtz in a fine-grained matrix of qtz, feldspar, biotite and chlorite with variably developed biotite foliation. Underlies Dean Quartzite.||||||
35317|Amputjuta Dacite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Part of the Pottoyu Granite Suite.  Finely porphyritic hypobyssal biotite dacite, less abundant equigranular leucogranite.  Age: ~1150Ma. Geological Province: Musgrave Block.||||||19-OCT-05
35317|Amputjuta Dacite|65256|2|Defined|piii, p7-8, p7 Tb.1, p30, p37|Stenian|Ectasian|New Name. Pb-Pb evaporation on zircon age. Previous informal name said to have been Manananna Porphyry (Forman 1966)[in fact Forman proposed the name Mannanana (sic) Porphyry in 1963]. Shallow level intrusive. Type locality 4.5 km SW of Amputjuta Outstation.|1153+/-3 Ma.|Of the Pottoyu Granite Suite.||Overlain by Kulail Sandstone, Dean Quartzite; intruded by mafic dykes interpreted to belong to Alcurra dolerite..|Porphyritic hypabyssal dacite with fine-grained phenocrysts of plagioclase; less abundant equigranular leucogranite.|26-MAR-15
35317|Amputjuta Dacite|69091|6|Mentioned|p139 Fig.6.6|||Mis-spelt as Amputjatja Dacite.||||||
35317|Amputjuta Dacite|69436|5|Briefly described|p21:9-10|Mesoproterozoic|Mesoproterozoic|Close et al. (2003). A hypabyssal intrusive unit in the Mannanana Range; geochemically equivalent to the rest of the Pottoyu Suite. Kober Pb-Pb zircon crystallisation age.|1153 +/- 5 Ma (Close et al., 2003).|Pottoyu Suite.||Is overlain by Dean Quartzite.|Contains phenocrysts of plagioclase and quartz in a fine-grained matrix of quartz, feldspar, biotite and chlorite, with a variably developed biotite foliation.|12-JUL-16
35317|Amputjuta Dacite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dacite|
35317|Amputjuta Dacite|71268|4|Described|1m_geologyp12_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen, Musgrave Province.||Unit of Pottoyu Granite Suite.|||Finely porphyritic hypabyssal dacite|
73998|Anchor Formation|14227|5|Briefly described|p11|Late Jurassic|Middle Jurassic|Geological Province: Exmouth Sub-basin. Marine shales.||||||07-FEB-11
25762|Anderson Formation|7142|6|Mentioned|p351. |||Canning Basin.||||||
25762|Anderson Formation|7433|6|Mentioned|p25 Fig.2, p31 Fig.7. |Early Carboniferous|Early Carboniferous|Fitzroy Graben, Canning Basin. Fine marine and continental clastics.||||||
25762|Anderson Formation|13234|6|Mentioned|p262 Tb.2|||Canning Basin.||||||
25762|Anderson Formation|13255|5|Briefly described|p368|Middle Carboniferous|Early Carboniferous|Oobagooma Sub-basin, Roebuck Basin.||||Overlies Laurel Formation.||29-SEP-15
25762|Anderson Formation|14228|6|Mentioned|p6 fig3|Carboniferous|Carboniferous|North Canning Basin.||||Overlies Fairfield Group.||
25762|Anderson Formation|22550|6|Mentioned|Fig 3|||||||||
25762|Anderson Formation|22718|6|Mentioned|P4|||||||||
25762|Anderson Formation|22741|5|Briefly described|P25, Table3 P15||Early Carboniferous|||||||
25762|Anderson Formation|22753|5|Briefly described|Fig.3 p585|Carboniferous|Carboniferous|||||||
25762|Anderson Formation|22764|4|Described|Table2,p10||Early Carboniferous|Age: ?500 m. Probably conformable on Laurel Formation and unconformable beneath Grant Formation||||||01-FEB-10
25762|Anderson Formation|22765|5|Briefly described|p6, Table1||Early Carboniferous|Maximum thickness of 2551m||||||30-OCT-15
25762|Anderson Formation|22767|5|Briefly described|Table3 P18, P21||Carboniferous|||||||
25762|Anderson Formation|22776|4|Described|Table.3|Early Carboniferous|Early Carboniferous|Fossil assemblage includes palynomorphs.||||||
25762|Anderson Formation|22814|5|Briefly described|fig2|Carboniferous|Carboniferous|||||||
25762|Anderson Formation|23356|5|Briefly described|26 Tab.2|Early Carboniferous|Early Carboniferous|||||||
25762|Anderson Formation|23523|5|Briefly described|p994 Fig. 2|Carboniferous|Carboniferous|||||||
25762|Anderson Formation|23766|4|Described|p14 Tb. 2|Early Carboniferous|Early Carboniferous|Comprises sandstone, siltstone and shale. Thickness: 1058m. See also p16.||||||17-FEB-10
25762|Anderson Formation|24061|4|Described|p181|Late Carboniferous|Late Carboniferous|Geological Province: Canning Basin. Maximum thickness: 1451m.||||||17-FEB-10
25762|Anderson Formation|24062|5|Briefly described|p186 Table 1|Carboniferous|Carboniferous|Geological Province: Canning Basin.||||||
25762|Anderson Formation|24246|5|Briefly described|p15|Carboniferous|Carboniferous|See also Anderson formation and Anderson Sandstone.||||||24-FEB-05
25762|Anderson Formation|24377|5|Briefly described|P13|Tournaisian|Tournaisian|Geological Province: Canning Basin.||||||11-APR-08
25762|Anderson Formation|24390|5|Briefly described|p6 Fig. 4|Carboniferous|Carboniferous|Geological Province: Canning Basin. Of the Fairfield Group. See also p8.||||||03-FEB-10
25762|Anderson Formation|29817|5|Briefly described|p8|||||||||
25762|Anderson Formation|29819|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
25762|Anderson Formation|30110|6|Mentioned|p81|||See also p82-83.||||||23-SEP-18
25762|Anderson Formation|30595|5|Briefly described|p3|||||||||
25762|Anderson Formation|30897|6|Mentioned|p19|||Subsurface unit||||||
25762|Anderson Formation|31706|6|Mentioned|p653|||U.Carb. Correlation Chart||||||
25762|Anderson Formation|32648|6|Mentioned|p32|||Carb.||||||
25762|Anderson Formation|33518|4|Described|Table 1|||||||||
25762|Anderson Formation|33519|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25762|Anderson Formation|33622|5|Briefly described|p89|||Early Carb. Continental drift.||||||
25762|Anderson Formation|33960|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25762|Anderson Formation|33965|6|Mentioned|p13|||||||||
25762|Anderson Formation|34085|6|Mentioned|Cor.chart|||Westphalian - Stephanian||||||
25762|Anderson Formation|34532|6|Mentioned|p219|||? Westphalian||||||
25762|Anderson Formation|35120|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25762|Anderson Formation|35124|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25762|Anderson Formation|35275|6|Mentioned|Fig.5.|||||||||
25762|Anderson Formation|35914|5|Briefly described|p6|||||||||
25762|Anderson Formation|36224|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Sandstone, siltstone, shale, minor limestone, dolomite, anhydrite.||||||01-FEB-05
25762|Anderson Formation|36225|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
25762|Anderson Formation|36257|6|Mentioned|Table 2.1|||||||||
25762|Anderson Formation|36365|6|Mentioned|p815|||||||||
25762|Anderson Formation|36634|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
25762|Anderson Formation|36890|3|Fully described|p338|||See also p344.||||||13-NOV-07
25762|Anderson Formation|38732|6|Mentioned|p33|||||||||
25762|Anderson Formation|38878|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25762|Anderson Formation|39757|6|Mentioned|p1606|||||||||
25762|Anderson Formation|40045|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25762|Anderson Formation|40078|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25762|Anderson Formation|40837|6|Mentioned|Fig.14|||||||||
25762|Anderson Formation|40838|6|Mentioned|p279|||||||||
25762|Anderson Formation|40992|6|Mentioned|p5|||Mention Fig.11||||||
25762|Anderson Formation|41169|6|Mentioned|p148|||||||||
25762|Anderson Formation|41271|6|Mentioned|p62|||||||||
25762|Anderson Formation|41436|6|Mentioned|p39|||||||||
25762|Anderson Formation|41454|6|Mentioned|p59|||||||||
25762|Anderson Formation|41589|6|Mentioned|p118|||||||||
25762|Anderson Formation|41688|5|Briefly described|Table 4|||||||||
25762|Anderson Formation|41730|6|Mentioned|p471|||||||||
25762|Anderson Formation|41839|3|Fully described|p25|||||||||
25762|Anderson Formation|42030|6|Mentioned|p747|||||||||
25762|Anderson Formation|42347|6|Mentioned|Fig.2 P1020|||||||||
25762|Anderson Formation|42547|4|Described|p96|||||||||
25762|Anderson Formation|42564|6|Mentioned|p11|||Fairfield Group.||||||
25762|Anderson Formation|42571|5|Briefly described|Table1 P9|||||||||
25762|Anderson Formation|42811|6|Mentioned|p51|||||||||
25762|Anderson Formation|42860|5|Briefly described|Fig.2|||||||||
25762|Anderson Formation|42880|5|Briefly described|Fig.2,p1020|||||||||
25762|Anderson Formation|42930|5|Briefly described|Fig.1 p473|Carboniferous|Early Carboniferous|Conformably overlies Yulleroo and Laurel Formations. Geological Province: Canning Basin. Deltaic and fluvial deposits.||||||13-NOV-07
25762|Anderson Formation|42933|5|Briefly described|Fig.94 p258|||||||||
25762|Anderson Formation|43173|6|Mentioned|12-54||Early Carboniferous|||||||
25762|Anderson Formation|43563|6|Mentioned|Fig.2,p4,5|Visean|Tournaisian|||||||
25762|Anderson Formation|43656|6|Mentioned|Fig.2,p8|Namurian|Tournaisian|||||||
25762|Anderson Formation|43666|6|Mentioned|p13|||||||||
25762|Anderson Formation|43746|6|Mentioned|Fig.2,p11|Namurian|Tournaisian|||||||
25762|Anderson Formation|43815|6|Mentioned|p93|||||||||
25762|Anderson Formation|43818|6|Mentioned|Fig.2.p39|Late Carboniferous|Early Carboniferous|||||||
25762|Anderson Formation|43932|5|Briefly described|p4,Tb.1 p7|||||||||
25762|Anderson Formation|44040|14|Not recorded|p43|||||||||
25762|Anderson Formation|44143|4|Described|p437 Table 4-19, p442, p443, p445|Early Carboniferous|Early Carboniferous|Up to 4000m thick. Sandstone, siltstone and shale; continental and marine. Disconformably(?) overlies Fairfield Group. Type section between 2408 and 3936m in Grant Range 1 (MOUNT ANDERSON 18deg 0' 48" S, 124deg 00' 22" E)||||||22-NOV-17
25762|Anderson Formation|44356|5|Briefly described|p9,Tb.1 p7||Early Carboniferous|||||||
25762|Anderson Formation|44998|2|Defined|p62,65,71,100-225|Stephanian|Westphalian|Underlies Grant Formation. See also App.6 p293.||||||
25762|Anderson Formation|45056|6|Mentioned|p58|||U.Carb.? Refers Balme (1960)||||||
25762|Anderson Formation|45063|6|Mentioned|Fig. 9|||Carb.||||||
25762|Anderson Formation|45097|6|Mentioned|Fig.|||Carboniferous correlation chart||||||
25762|Anderson Formation|45133|6|Mentioned|p2|||||||||
25762|Anderson Formation|45143|6|Mentioned|p4|||||||||
25762|Anderson Formation|45153|2|Defined|App.3-35|Early Carboniferous|Early Carboniferous|||||||
25762|Anderson Formation|45158|3|Fully described|p22|||||||||
25762|Anderson Formation|46794|5|Briefly described|p63|||||||||
25762|Anderson Formation|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
25762|Anderson Formation|48573|2|Defined|p.3,9,15,21|||(E51-7/Alexander Creek).||||||13-NOV-07
25762|Anderson Formation|48971|6|Mentioned|p27|||See also p36.||||||23-SEP-18
25762|Anderson Formation|48978|6|Mentioned|p4|||Conformable on Laurel Fm.||||||
25762|Anderson Formation|50085|5|Briefly described|p6 Fig. 4|Early Carboniferous|Early Carboniferous|Geological Province: Canning Basin.||||||
25762|Anderson Formation|60386|6|Mentioned|p297|Carboniferous||Roebuck/Canning Basin. Shown as pre-Alice Springs Orogeny.||||||
25762|Anderson Formation|61021|5|Briefly described|p36 Fig. 2|Namurian|Visean|Geological Province: Canning Basin. See also p39.||||||17-DEC-07
25762|Anderson Formation|61023|5|Briefly described|p10 Fig. 6|Carboniferous|Carboniferous|Geological Province: Canning Basin.||||||11-APR-08
25762|Anderson Formation|61551|6|Mentioned|p351 Fig.2, p355, p359, p361. |Serpukhovian|Tournaisian|Canning Basin. Oil sourced from the Laurel Formation is produced from this unit at the Lloyd and West Kora fields.||||||
25762|Anderson Formation|62837|5|Briefly described|Stratigraphic columns|Early Carboniferous|Early Carboniferous|Age: 347-323. Geological Province: Fitzroy Trough.||||||01-MAR-10
25762|Anderson Formation|64187|5|Briefly described|p320 Fig. 2|Permian|Early Carboniferous|Underlain by Laurel Formation, overlain unconformably by Grant Formation. Sandstone, shale, siltstone (continental-estuarine). Geological Province: Canning Basin.||||||03-FEB-10
25762|Anderson Formation|64643|5|Briefly described|p3 Fig. 2|Missippippian|Missippippian|||||||
25762|Anderson Formation|64971|5|Briefly described|p683, p684, p685, p685 Fig. 2|Early Carboniferous|Early Carboniferous|Overlian unconformably by Reeves Formation, underlain by Fairfield Group. See also p689 Fig. 6.||||||09-FEB-10
25762|Anderson Formation|64981|5|Briefly described|p669 Fig.3.|Late Carboniferous|Visean|Clastic marginal marine to deltaic regressive episode, representing a phase of rift infill. Locally entirely eroded at end of mid-Carboniferous. Oil-bearing in the Lloyd oil field; sealed by intraformational shales.||||Overlies Fairfield Group. Is unconformably overlain by Betty Formation of Grant Group.|Mainly sand, with minor carbonate.|
25762|Anderson Formation|65301|5|Briefly described|p5 Fig. 4|Mississippian|Mississippian|Geological province: Canning Basin.||||||
25762|Anderson Formation|65382|5|Briefly described|p714, p717 App. 2|Namurian|Visean|Canning Basin. Age of >/= 327 Ma and Visean/Namurian given. 327 Ma corresponds to Serpukhovian on current international timescale.||||||
25762|Anderson Formation|65449|5|Briefly described|p5-6|Early Carboniferous|Early Carboniferous|Fitzroy Trough and Gregory Sub-basin, Canning Basin. Deltaic siliciclastic rocks. Top of Megasequence II of Warris (1993).||||Overlies Laurel Formation (Fairfield Group).||
25762|Anderson Formation|66949|4|Described|p58 App.3, p3, p4 Fig.2, p8, p28, p34,|Visean|Visean|See also p50 Appx.2; p76-79,81-82,87,90,94 Appx.5. Type section in Grant Range 1, 2404-3936m. Age from palynology, presumably in upper part of unit. Up to 1800m thick; continental - marine deposits. Includes the Grandispora maculosa zone (Kemp, 1977). Available core detailed.||||Conformably overlies Fairfield Group. Is overlain ?unconformably by Reeves Formation.|Sandstone, siltstone and shale; coal seams. Intersections of dolerite (Barlee 1 well) and gabbro (Fraser River 1 well).|30-OCT-15
25762|Anderson Formation|68007|6|Mentioned|p4|Carboniferous|Carboniferous|Canning Basin.||||||
25762|Anderson Formation|68902|6|Mentioned|p9 fig 5|Carboniferous|Carboniferous|||||Overlies Laurel Formation. Is overlain unconformably by Reeves Formation.||
25762|Anderson Formation|69029|5|Briefly described|p319,322|Visean|Tournasian|Of Canning Basin. Reservoirs in the Anderson Formation are sealed by interbedded basinal shales and tight limestones in the Laurel Formation and equivalents.||||Overlain by Reeves Formation. Underlain by Fairfield Group.||
25762|Anderson Formation|69182|5|Briefly described|Ch4 p9, Ch4 p13-p14, Ch4 p30-p36|Visean|Visean|North Canning Basin. Potential seal for the storage of carbon dioxde. See also Ch4 p38-p39, Ch4 p42, Ch4 p44, Ch4 p45, Ch4 p47, Ch4 p50-p58, Ch4 p62-p65, Ch4 p67, Ch4 p74-p77, Ch4 p83-p84, Ch4 p88, Ch4 p90, Ch4 p96.   ||||Unconformably overlies the Laurel Formation. Unconformably overlain by the Reeves Formation.|Fluvio-deltaic sandstones.|
25762|Anderson Formation|69297|6|Mentioned|p351, p354, 355|Early Carboniferous|Early Carboniferous|Canning Basin. ||||Overlies the Laurel Formation.||23-SEP-18
25762|Anderson Formation|69312|6|Mentioned|p3, p15, p19, p25 fig 31|Serpukhovian|Tournaisian|Canning Basin. See also p29 fig 37, p30. ||||Overlies the Laurel Formation. Faulted against the Reeves Formation [?].|Shale and sandstone.|11-FEB-20
25762|Anderson Formation|69693|6|Mentioned|p3-4|Carboniferous|Carboniferous|Canning Basin. Visean.||||Overlies Fairfield Group. Is overlain unconformably by Betty Formation (Grant Group).||
25762|Anderson Formation|70492|6|Mentioned|p166, 176-181|Early Carboniferous|Early Carboniferous|Canning Basin. Well logs, biostratigraphy.||||Overlies Fairfield Group. Is overlain unconformably by Grant Group.|Fluvio-deltaic siliciclastics.|
25762|Anderson Formation|70774|5|Briefly described|p4, p9|Mississippian|Mississippian|Fitzroy Trough and Lennard Shelf, Canning Basin.||||Overlies the Laurel Formation. Unconformably overlain by the Reeves Formation.||
25762|Anderson Formation|71146|5|Briefly described|p6, p34,  p43 fig 33|Visean|Tournaisian|Canning Basin. Believed to be partially equivalent to the Williambury Formation.||||Unconformably overlies the Fairfield Group. Unconformably overlain by the Reeves Formation.|Sandstone.|
25762|Anderson Formation|71233|5|Briefly described|p103, p115|Tournaisian|Tournaisian|Canning Basin sub-surface. Age relations with NSW microflora discussed.||||||
25762|Anderson Formation|71870|6|Mentioned|p3|Visean|Tournaisian|Canning Basin.||||Overlain by the Reeves Formation. Overlies the Fairfield Group.||
25762|Anderson Formation|71894|5|Briefly described|p3-p4|Visean|Tournaisian|Canning Basin; only present in  the north of the basin based on well intersections.||||Unconformably overlies the Laurel Formation. Unconformably overlain by the Reeves Formation.|Sandstone and shale.|
25762|Anderson Formation|72496|5|Briefly described|p219-220, p223-224, p226-227, 229|Visean|Visean|Canning Basin. Characterised by medium to high gamma ray readings. Deposited in a fluvial environment. Displays medium to high amplitude seismic reflections.||||Overlain by the Reeves Formation. Overlies the Fairfield Group.|Dominantly sandstone with some siltstone and minor mudstone..|18-MAR-20
25762|Anderson Formation|72497|5|Briefly described|p3 Fig.2, p17 Fig.11.|Visean|Tournasian|Canning Basin. Shown as occuring in the Fitzroy Trough, Betty and Balgo Terraces and part of the Lennard Shelf and Margaret Terrace.||||Conformably to unconformably overlies Fairfield Group. Unconformably underlies Grant Group.||
25762|Anderson Formation|72499|4|Described|p7 Fig.6, p62-3 Fig.54, p94.|Visean|Tournaisian|Located in the Fitzroy Trough. Early Carboniferous pollen (G.frustulentus) identified in core log (Scarpia 1.) at 1531m depth.||||Overlies Laurel Formation and shown as  unconformably overlying Fairfield Group.  Shown as unconformably underlying Reeves Formation.|Includes sandstone and some carbonate shale.|
25762|Anderson Formation|72502|6|Mentioned|p5|Visean|Visean|Lennard Shelf and Fitzroy Trough, Canning Basin.||||||
25762|Anderson Formation|72504|6|Mentioned|Figure 1-2|||Overlain by Reeves Formation in Grant Range 1, East Yeeda 1 and Fraser River 1? Overlain by Grant Group in Kilang Kilang 1?||||||18-MAR-20
25762|Anderson Formation|73117|5|Briefly described|[See comments].|Visean|Visean|Hydrocarbon source interval. Lies within the G. frustulentus Microflora. Capped by the regionally extensive Meda unconformity. Can be difficult to differentiate from the Reeves Formation in the absence of biostratigraphic data. Includes well-dated marine faunas. Upper boundary marked by the Meda Transpression. p: 1, 3, 12, 15-17, 19, 21, 32, 38-39, 54, 70, 109, 111, 113-115, 117-121, 123-124, 127-128, 130-132, 135-140, 142.||||Unconformably overlain by Reeves Formation. Unconformably? underlain by Fairfield Group including Laurel Formation.|Dominated by sandstone with lesser mudstone and minor limestone.|
31682|Andover Intrusion|23793|5|Briefly described|p29|||Informal||||||
31682|Andover Intrusion|24024|5|Briefly described|Map Legend|Archean|Archean|Informal name - structural term, not stratigraphic. Of the Pilbara Supergroup. Geological Province: Pilbara Craton||||||07-NOV-08
31682|Andover Intrusion|24353|5|Briefly described|p5|Archean|Archean|Age: >2990Ma. Geological Province: Pilbara Craton||||||07-NOV-08
31682|Andover Intrusion|43822|5|Briefly described|map legend|Archean|Archean|Layered mafic intrusions approx. 2925 Ma. In the Pilbara Supergroup.||||||07-NOV-08
31682|Andover Intrusion|63441|5|Briefly described|p10 Tb. 2|Archean|Archean|Of the Orpheus Supersuite. Age :c.3016Ma. Geological province: Pilbara Craton.||||||07-FEB-11
31682|Andover Intrusion|64174|5|Briefly described|Map legend|Archean|Archean|Of the Orpheus Supersuite. Geological province: Pilbara Craton. Gabbro, leucograbbro, serpentinised peridotite and dunite, pyroxenite and minor anorthosite; metamorphosed.||||||08-DEC-08
31682|Andover Intrusion|64580|4|Described|map legend|Mesoarchean|Paleoarchean|Of Orpheus Supersuite. Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed.||||||15-DEC-08
31682|Andover Intrusion|67201|4|Described|p16-17 Fig.9, p23, p25, p27, p67|Archean|Archean|Pilbara Craton. In Roebourne-Karratha area. A layered ultramafic-mafic intrusion, located south of Roebourne. Though another possibility is that this is a faulted section of c. 3120 Ma Bullock Hide Intrusion (Railway Supersuite).||Orpheus Supersuite||Overlies Ruth Well Formation.|Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed. Amphibolite (metabasalt).|
31682|Andover Intrusion|69185|4|Described|500k_geologyp08_lut.csv|Mesoarchean|Paleoarchean|Geological province: West Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|>3016 Ma|Unit of Orpheus Supersuite.|||Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed|
31682|Andover Intrusion|69300|5|Briefly described|map legend|Archean|Archean|West Pilbara Granite-Greenstone Terrane|>3016 Ma, interp. geochron. age, Nelson 2001||||undivided gabbro, mafic, and ultramafic rocks forming layered sills; metamorphosed|
31682|Andover Intrusion|70775|5|Briefly described|iii, p15, p23, p46, p49, p66, p73, p94|||Pilbara Craton. This is the largest layered intrusion of the northern Pilbara Craton and occupies an area of about 200 square km.||Orpheus Supersuite||Intrudes the Weerianna Basalt.|Gabbro, leucogabbro, serpentinized peridotite, dunite, lherzolite, olivine websterite, clinopyroxenite, orthopyroxenite, websterite, pyroxenite and minor anorthosite; metamorphosed.|
31682|Andover Intrusion|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||gabbro, dolerite, anorthosite, pyroxenite|
31682|Andover Intrusion|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|De Grey Superbasin.||Orpheus Supersuite|||Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed.|
79060|Angas Hills Formation|70762|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Amadeus Basin, Centralian Superbasin.|||||Interbedded conglomerate and sandstone, minor mudstone.|07-NOV-16
79060|Angas Hills Formation|70839|5|Briefly described|p328-333,335,337-340|Cambrian|Ediacaran|Of Amadeus Basin. Part of Supersequence 4. Thickness: >300m.  SHRIMP U-Pb zircon geochronology samples and analysis on p331-334. Concordant dates between c. 2459 and c. 781 Ma. Dominant age component between c. 1.23 and c. 1.09 Ga, with a smaller  oncentration of latest Palaeoproterozoic to early Mesoproterozoic ages (c. 1.7-1.4 Ga), and four early Neoproterozoic zircons.|Max dep age: 781+\-24 Ma (238U/206Pb)|||Underlain by Bitter Springs Formation.|Fluvial sandstone and conglomerate succession.|
79060|Angas Hills Formation|71088|2|Defined|p1-p2, p7-p8, p12, p14, p16|Cambrian|Ediacaran|Amadeus Basin. Previously the Angas Hills beds of Blake and Tower, 1974. Proposed by Peter Haines and Heidi Jane Allen (GSWA). Name is derived from Angas Hills (late 25'52'S, long 128'9'E). The type locality is a cliff section 36m high in eastern Angas Hills (lat 22'51'00"S long 128'12'30"E); this locality was previously the reference section of Blake and Towner (1974) elevated as no type locality had been proposed. Reassigned to Supersequence 4. This unit is restricted to outliers of the Amadeus Basin within the Arunta Region on the southern half of the WEBB (1:250k). Geomorphic expression is low hills, scarps, rises and plateaus. Blake (1977) suggested a Paleozoic age and correlation with the Pertnjara Group. Haines et al (2010a, b; 2012) suggested an Ediacaran to Cambrian age on the basis of lithological similarities, clast assemblage and paleocurrent measurements. Sedimentary facies suggest a fluvial depositional environment. Outcrops are typically flat-lying to gently dipping and are locally upturned near faults. An estimated thickness of 300m was provided from Blake and Towner (1974); at the type locality 36m is exposed. Sample description and locality are provided. References are provided. See also  p18-p21, p23-p25, p32-p33.||||Unconformably overlies the Heavitree Quartzite and the Bitter Springs Formation. Equivalent to the Carnegie Formation and the Maurice Formation.|Coarse pebble conglomerate with thin lenses and layers of clayey sandstone overlain by partly pebbly cross-bedded sandstone.|
79060|Angas Hills Formation|71800|5|Briefly described|p26-p27|Early Cambrian|Ediacaran|Amadeus Basin.||||Overlies the Julie Formation. Overlain by the Todd River Dolostone.|Lithic sandstone.|
23335|Angel Formation|12498|5|Briefly described|pp515-526.|Late Jurassic|Late Jurassic|Late Tithonian extensive submarine fan sandstones; contained an 11 m oil column found in Lambert 1 discovery well in 1973. Lambert 2 in 1996 met a separate, gross 37 m oil-bearing interval and a 133 m gas column in the lower-lying North Rankin Formation.|||||Clean, fine- to medium-grained sandstones, with subordinate shale interbeds to 5 m thick and heavily bioturbated.|
23335|Angel Formation|23726|5|Briefly described|p8 Fig 2c|Jurassic|Jurassic|Underlying unit Legendre Formation. Geological Province: Carnarvon Basin.||||||
23335|Angel Formation|24390|5|Briefly described|p22|Late Jurassic|Late Triassic|Geological Province: Northern Carnarvon Basin.||||||
23335|Angel Formation|40617|2|Defined|p10|Middle Jurassic|Early Jurassic|Early to Middle Jurassic||||||01-SEP-14
23335|Angel Formation|41271|3|Fully described|p130|||See also type section mislabelled Locker Shale. Comment from 93/27545 p36.||||||
23335|Angel Formation|41436|6|Mentioned|p47|||||||||
23335|Angel Formation|41438|6|Mentioned|p106|||See also p108||||||04-JAN-18
23335|Angel Formation|41440|6|Mentioned|p136|||||||||
23335|Angel Formation|41732|6|Mentioned|p534|||||||||
23335|Angel Formation|42116|5|Briefly described|Fig.1 P6|||||||||
23335|Angel Formation|42598|6|Mentioned|P 43|Jurassic||||||||
23335|Angel Formation|42615|3|Fully described|p35|||Age early Kimmeridgian to latest Tithonian||||||
23335|Angel Formation|43712|6|Mentioned|p11|||||||||
23335|Angel Formation|43722|6|Mentioned|p10|||||||||
23335|Angel Formation|43724|6|Mentioned|p29|||||||||
23335|Angel Formation|43826|6|Mentioned|Fig.2,p163||Late Jurassic|||||||01-MAR-10
23335|Angel Formation|44937|5|Briefly described|p90,99||Late Jurassic|Tithonian age||||||
23335|Angel Formation|50085|5|Briefly described|p24 Tb. 6|Late Jurassic|Late Jurassic|Geological Province: Northern Carnarvon Basin (Dampier Sub-basin).  See also p22.||||||
23335|Angel Formation|60379|5|Briefly described|p126 fig 3, p127, 128|Early Cretaceous|Tithonian|Dampier sub-basin, Carnarvon Basin. Hydrocarbon play sealed by Forestier Claystone.|||||Sandstone|
23335|Angel Formation|60386|6|Mentioned|p302|Early Cretaceous|Late Jurassic|Mis-spelt as Angei Formation. Northern Carnarvon Basin. ||||||
23335|Angel Formation|61023|6|Mentioned|p29|Late Triassic|Late Jurassic|||||||
23335|Angel Formation|62837|5|Briefly described|Stratigraphic columns|Oxfordian|Oxfordian|Age: >145Ma. Geological Province:  Barrow and Dampier Sub-basins, Rankin Platform and Beagle Sub-basin.||||||01-MAR-10
23335|Angel Formation|63950|5|Briefly described|p336 Fig. 4, p338|Tithonian|Kimmeridgian|Geological Province: northern Carnarvon Basin. Fluvial and shallow marine sequences.||||||27-MAY-08
23335|Angel Formation|64693|6|Mentioned|p389, |||Dampier Sub-basin. ||||||
23335|Angel Formation|64978|6|Mentioned|p528 Fig.2.|Late Jurassic|Late Jurassic|||||||
23335|Angel Formation|66126|6|Mentioned|p206|Late Jurassic|Late Jurassic|Carnarvon Basin.||||||
23335|Angel Formation|67200|5|Briefly described|p8 fig 6, |Late Jurassic|Late Jurassic|||||Overlies Legendre Formation|Sandstone and silstone.|18-SEP-18
23335|Angel Formation|67368|5|Briefly described|p209 Fig.4, p210 Fig.5.|Late Jurassic|Late Jurassic|||||Overlies Dingo Formation. Is overlain by Forestier Claystone.|Turbidite sandstone.|
23335|Angel Formation|68135|5|Briefly described|p51 Fig.2a|Early Cretaceous|Late Jurassic|Northern Carnarvon Basin.||||Is overlain unconformably by Barrow Group.||13-SEP-17
23335|Angel Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Northern Carnarvon Basin.||||Overlies Angel Formation.||
23335|Angel Formation|70066|5|Briefly described|Dampier: Fig.2; p2. Exmouth: Fig.2|Berriasian|Oxfordian|See also Regional: Fig.6; p6, p11. Northern Carnarvon Basin. These turbidites constitute the main oil and gas-bearing reservoir unit in the Dampier Sub-basin.||||Overlies Calypso Formation, as well as Dingo Claystone with which it is also interbedded. Is overlain by Forestier Claystone.||
77463|Anjo Sandstone Member|67370|6|Mentioned|p313 Fig.2. |Early Triassic|Early Triassic|||||||
23337|Anna Plains Sandstone|40793|6|Mentioned|p164|||||||||
23337|Anna Plains Sandstone|40837|6|Mentioned|p260|||||||||
23337|Anna Plains Sandstone|41215|6|Mentioned|Fig.4|||||||||
23337|Anna Plains Sandstone|64783|5|Briefly described|p93|||Canning Basin.||||Correlates with the Log Creek Formation.||15-NOV-17
23337|Anna Plains Sandstone|66127|5|Briefly described|p441.|Early Givetian|Middle Eifelian|Pre-reef, subsurface strata in Canning Basin. Contains miospores from the Euramerican devonicus-naumovae zone.||||||31-JAN-14
36842|Annabelle Volcanics|23727|4|Described|p10|Archean|Archean|Geological Province: Ravensthorpe Terrane.||||||07-NOV-08
36842|Annabelle Volcanics|23728|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Manyutup Tonalite Complex. Geological Province: Yilgarn Craton.||||||07-NOV-08
36842|Annabelle Volcanics|23752|4|Described|p7|Archean|Archean|Geological Province: Ravensthorpe Terrane.||||||07-NOV-08
36842|Annabelle Volcanics|23753|5|Briefly described|Map Legend|Archean|Archean|Calc-alkaline volcanic association.  Geological Province: Yilgarn Craton.||||||07-NOV-08
36842|Annabelle Volcanics|23754|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Yilgarn Craton.||||||10-FEB-14
36842|Annabelle Volcanics|24165|6|Mentioned|p31, p53|||Hosts most gold and base metal mineralisation in the Ravensthorpe and Cocanarup areas, within 2km of contact with Manyutup Tonalite.||||||
36842|Annabelle Volcanics|50542|5|Briefly described|p122|Archean|Archean|Comprising of metamorposed ultramafic, mafic and felsic volcanic rocks. Geological Province: Yilgarn Craton. Host the Cattlin Creek Pegmatite.||||||07-FEB-11
36842|Annabelle Volcanics|64580|4|Described|map legend|Archean|Archean|Metamorphosed dacitic and andesitic volcaniclastics and volcanics; minor basalt and rhyolite.||||||15-DEC-08
36842|Annabelle Volcanics|65487|5|Briefly described|p6|||Included in the Ravensthorpe Suite, thought to be co-magmatic with the Manyutup Tonalite. Aged 2966 +/- 12 Ma (Savage et al., 1996) from the tonalite. Stratigraphically complex - includes: dominant volcaniclastics, and minor lavas: metamorphosed calc-alkaline basalts (10-20%), andesite (50-70%), and dacite (20-30%).||||||10-FEB-14
36842|Annabelle Volcanics|69404|5|Briefly described|p10|||Ravensthorpe Terrane. |||||Andesitic to dacitic agglomerates and tuffs with minor basalts.|
36842|Annabelle Volcanics|69559|5|Briefly described|500k_geologyp08_lut.csv|Archean|Archean||||||Metamorphosed dacitic to andesitic volcaniclastics and volcanics; minor basalt and rhyolite.|
36842|Annabelle Volcanics|69617|6|Mentioned|p155|||Ravensthorpe greenstone belt, Southern Cross Domain.|2989 +/- 11 Ma (Witt, 1999).|||||08-FEB-17
36842|Annabelle Volcanics|70020|6|Mentioned|p127|Mesoarchean|Mesoarchean|Hosts Cu-Au mineralisation.|2989+\-11 Ma|||||
36842|Annabelle Volcanics|70156|4|Described|500k_interpgeop14_lut.csv|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Youanmi Terrane events (3200-2600 Ma).|2958+\-4 Ma (isotopic)||||Metamorphosed dacitic and andesitic volcaniclastic and volcanic rocks; minor basalt and rhyolite|
36842|Annabelle Volcanics|70794|4|Described|500k_interpgeop14_lut.csv|Mesoarchean|Mesoarchean|Youanmi Terrane, Yilgarn Craton. Also 2_5m_interpgeop15_lut.csv.|2958+/-4 Ma||||Metamorphosed dacitic and andesitic volcaniclastic and volcanic rocks; minor basalt and rhyolite.|
36842|Annabelle Volcanics|70802|5|Briefly described|500k_interpgeop14_lut.csv|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Youanmi Terrane events.|2958+\-4 Ma||||Metamorphosed dacitic and andesitic volcaniclastic and volcanic rocks; minor basalt and rhyolite|
36842|Annabelle Volcanics|71168|5|Briefly described|p17, p50|||Ravensthorpe greenstone belt. Together with the Manyutup Tonalite forms the Ravensthorpe 'Terrane'. Hosts significant syn-volcanic copper-gold and copper-zinc mineralization..|2989 +/- 11 Ma (U-Pb, Savage et al., 1995)||||Volcaniclastic rocks with less abundant lava flows consisting primarily of basalt to minor rhyolite, dominantly andesites, and minor dolerite.|
36842|Annabelle Volcanics|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Youanmi Terrane.|2958+/-4 Ma.||||Metamorphosed dacitic and andesitic volcaniclastic and volcanic rocks; minor basalt and rhyolite.|
36842|Annabelle Volcanics|72491|5|Briefly described|p46|||NW Ravensthorpe Belt. Appears as Annabelle volcanics. Metamorphic effects described.|||||Aluminous metapelite.|
74813|Annean Supersuite|30|5|Briefly described|p191-192|Neoarchean|Mesoarchean|Geological province: Murchison Domain, Yilgarn Craton. Comprises plutonic bodies interpreted to be subvolcanic intrusions to Polelle group felsic volcanic centres (Van Kranendonk et al., 2010).|2785-2733 Ma||Includes Eelya Suite, Cullculli Suite and Mount Kenneth Suite, and Nanine Tonalite.|||
74813|Annean Supersuite|64891|4|Described|p34 Fig. 1, p37 Fig. 2, p41, p48-9 Tb. 1|Archean|Archean|Includes Cullculli + Eelya Suites (granites) and Meeline+Boodanoo Suites (mafic-ultramafic). Age: 2787-2733Ma. Geol.prov: Murch.Dom. Syn-volcanic tonalitic rocks+trondhjemite, granodiorite, gabbro, peridotite, dolerite, pyroxenite, magnetite, anorthosite||||||07-FEB-11
74813|Annean Supersuite|65548|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Youanmi Terrane, Yilgarn Craton. Includes unnamed units of the Cullculli Suite which have dates of 2740 Ma, 2730 Ma.||||||14-APR-11
74813|Annean Supersuite|66195|5|Briefly described|p599 Fig.2|||Contains the Cullculli Suite and the Eelya Suite.||||||13-MAR-12
74813|Annean Supersuite|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|||Includes Cullculli Suite and Gnanagooragoo Igneous Complex, and ten separately-mapped but un-named units.||Metatonalite, dolerite; metagranite with abundant pegmatite, metamonzogranite with slivers of felsic schist, biotite metagranodiorite, granitic gneiss, biotite tonalite gneiss, granite dykes in greeenstones.|
74813|Annean Supersuite|67129|5|Briefly described|p18 Fig.19, p18 Fig.20, p30, p33-34, p46|Archean|Archean|Murchison Domain, Youanmi Terrane. REE plot; geochemical modelling.|2805-2735 Ma||Cullculli, Eelya, Little Gap, Boodanoo, Meeline Suites; Mindoola, Racecourse Tonalites.||Comprises granites which fall into three distinct compositional groups: 1. highly fractionated REE and no Eu anomaly 2. slightly flatter REE than group one with small negative Eu anomalies. 3. Higher HREE and large negative Eu anomaly.|06-SEP-17
74813|Annean Supersuite|68107|6|Mentioned|p618|||Western Youanmi Terrane.|||Includes Cullculli Suite.|||
74813|Annean Supersuite|68108|5|Briefly described|p628, p649|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane.|ca. 2785-2733 Ma||||Syn-volcanic tonalites.|
74813|Annean Supersuite|68287|5|Briefly described|Map Legend|Archean|Archean|Metamorphosed.|||Includes Mount Kenneth Suite, Meeline Suite.|||
74813|Annean Supersuite|68519|5|Briefly described|Map Legend|Neoarchean||Murchison Domain, Youanmi Terrane, Yilgarn Craton.|||Includes Meeline Suite.|||
74813|Annean Supersuite|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane. Age 2787-2744 Ma, from Geochron file 178141.1.pdf. Age 2805 - 2730 Ma from 185920.1.pdf. Age 2887-2733 Ma from geochron file 185926.1.pdf, 185958.1.pdf etc. 2815-2730 Ma from geochron file 193967.1.pdf|most recent age range:  2815-2730 Ma||Includes Gnanagooragoo Igneous Complex, Cullculli Suite, Mount Kenneth Suite, Boodanoo Suite, Meeline Suite, Eelya Suite and 11 unnamed units.|Intrudes Norie and Polelle Groups (Murchison Supergroup).|Metagranite; granite gneiss; granite; Amphibolitic metadolerite; metatrondhjemite; Serpentinite; Metagabbro; Dolerite; Gabbronorite; Schist; Metapyroxenite; Anorthosite; Troctolite; Metadunite; Peridotite; Magnetitite; Dunite; norite; troctolite;|
74813|Annean Supersuite|68698|5|Briefly described|p4-5, p7-11, p13-18, p27-28, p33-34|Neoarchean|Mesoarchean|Northern Murchison Domain. A major plume event produced the early components of this unit. Emplacement was synchronous with deposition of the Norie and Polelle Groups. A granite orthogneiss was dated at 2744 +/- 3 Ma (Wingate and Van Kranendonk, 2009); a monzogranite with mafic clots at 2748 +/- 2 Ma (Wingate et al., 2011). Geochemistry is discussed in detail. Lu-Hf isotope data and source regions discussed.|c.2815-2735 Ma.||Mount Kenneth, Cullculli, Eelya, Meeline and Boodanoo Suites.|Intrudes Polelle Group.|Metamorphosed felsic and mafic intrusive rocks.|
74813|Annean Supersuite|69014|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane.|||Includes the Mount Kenneth Suite and the Meeline Suite.|||18-NOV-13
74813|Annean Supersuite|69583|4|Described|p49, p51-52, p126; Plate 2|Neoarchean|Mesoarchean|Murchison Domain. Widespread synvolcanic granitic/tonalitic rocks: coeval with Norie and Polelle Groups. Age also given as 2785-2733 Ma.|c.2815-2740 Ma.||Boodanoo, Mount Kenneth, Cullculli, Eelya, Meeline Suites; Gnanagooragoo Igneous Complex.|Overlies and intrudes Glen Group.|Metamorphosed granitic and gabbroic rocks.|
74813|Annean Supersuite|69584|6|Mentioned|p2, p5 Fig.2, Plate 1|Neoarchean|Mesoarchean||||Mount Kenneth Suite, Cullculli Suite, Eelya Suite||Mafic igneous rocks.|
74813|Annean Supersuite|69586|5|Briefly described|p22|Neoarchean|Mesoarchean|Murchison Domain.|||Mount Kenneth, Cullculli, Eelya Suites.|||
74813|Annean Supersuite|69626|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton|||Mount Kenneth Suite, Boodanoo Suite, Meeline Suite|||
74813|Annean Supersuite|69627|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton|||Cullculli Suite|||
74813|Annean Supersuite|69628|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton|||Meeline Suite|||
74813|Annean Supersuite|69744|6|Mentioned|p254||||2815-2735 Ma.|||||
74813|Annean Supersuite|70020|5|Briefly described|p118|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton.|||Includes Eelya, Cullculli and Mount Kenneth suites.|Overlain by Austin Downs Supersuite.||
74813|Annean Supersuite|70030|5|Briefly described|p191-192|Neoarchean|Mesoarchean|Geological province: Murchison Domain, Yilgarn Craton.|||Includes Eelya Suite, Cullculli Suite and Mount Kenneth Suite, and Nanine Tonalite.||Tonalitic rocks.|17-JUL-19
74813|Annean Supersuite|70139|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton. All six facies are mapped separately.|||Eelya Suite.||Granodiorite; amphibole-rich tonalite, locally sheared; K-feldspar and quartz porphyritic biotite monzogranite, strongly foliated; mafic intrusive rock: mainly gabbro, minor leucogabbro and dolerite; dolerite; biotite granodiorite; all metamorphosed.|
74813|Annean Supersuite|70140|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. 16 un-named facies, of metamorphosed mafic and ultramafic rocks, are mapped separately.|||Meeline, Mount Kenneth Suites.|||
74813|Annean Supersuite|70153|6|Mentioned|500k_interpgeop14_lut.csv|Neoarchean|Mesoarchean||||Includes Cullculli Suite|||
74813|Annean Supersuite|70226|5|Briefly described|map legends|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Carton.|2801-c.2742 Ma.||Rothsay, Warriedar Suites.|||16-DEC-15
74813|Annean Supersuite|70418|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|2820-2735 Ma.||||Fine-grained biotite tonalite gneiss; includes cross-cutting younger phases and pegmatites.|
74813|Annean Supersuite|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton.|c.2813-c.2749 Ma.||Meeline, Warriedar, Rothsay Suites; Edamurta Gabbro.|||
74813|Annean Supersuite|70770|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|||Mount Kenneth, Rothsay Suites.|||
74813|Annean Supersuite|70796|4|Described|2_5m_interpgeop15_lut.csv|Neoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. Affected by the Yilgarn Craton granite magmatism (3010  2600 Ma); Youanmi Terrane events (3131  2600 Ma). See also 100k_geologyl_lut.csv, 100k_geologyp_lut.csv, 100k_geologysub_lut.csv. 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 155822.pdf, 155879.1.pdf, 178141.1.pdf, 178194.1.pdf, 178196.1.pdf, 185920.1.pdf, 185921.1.pdf, 185926.1.pdf, 185928.1.pdf, 185933.1.pdf, 185958.1.pdf, 185995.1.pdf, 185996.1.pdf, 193967.1.pdf, 194747.1.pdf, 194749.1.pdf, 194751.1.pdf, 194757.1.pdf, 198210.1.pdf, 198294.1.pdf, 203702.1.pdf, 203703.1.pdf, 203704.1.pdf, 211102.1.pdf, Austin100_2442_stratig.pdf, Badja100_2240_stratig.pdf, Bungar100_2539_stratig.pdf, Challa100_2541_stratig.pdf, Coolamaninu100_2540_stratig.pdf, Cue100_2443_stratig.pdf, Madoonga100_2444_stratig.pdf, MountMagnet100_2441_stratig.pdf, Nowthanna100_2643_stratig.pdf, Reedy100_2543_stratig.pdf, Windimurra100_2641_stratig.pdf, Wynyangoo100_2542_stratig.pdf, Yalgoo100_2241_stratig.pdf, Youanmi100_2640_stratig.pdf. Numerous additional lithologies are discussed.|ca 2820 to 2735 Ma (inferred)||Includes the Gnanagooragoo Igneous Complex, Edamurta Gabbro, Cullculli Suite, Rothsay Suite,  Warriedar Suite, Boodanoo Suite, Mount Kenneth Suite, Eelya Suite and the Meeline Suite.|Intrudes the Norie and Polelle groups.|Metamonzogranite, monzogranite, metagranite, and weakly metamorphosed layered mafic-ultramafic intrusions; granitic rocks commonly foliated|15-DEC-22
74813|Annean Supersuite|70830|4|Described|p8-p9, p58|Neoarchean|Neoarchean|Murchison Domain. |c. 2785-2733 Ma||Includes the Mount Kenneth Suite, Meeline Suite, Boodanoo Suite, Cullculli Suite, Warriedar Suite, Rothsay Suite and the Eelya Suite.||Tonalitic rocks.|
74813|Annean Supersuite|71159|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|c.2813 Ma.||Meeline, Mount Kenneth Suites.|||
74813|Annean Supersuite|71168|5|Briefly described|p7|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c. 2810-2740 Ma||Includes the Mount Kenneth Suite, Cullculli Suite and the Eelya Suite.||Granitic rocks.|
74813|Annean Supersuite|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Includes the Gnanagooragoo Igneous Complex. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). Sample GSWA 194757 (metadolerite of Gnanagooragoo Igneous Complex) yielded a weighted mean 207Pb/206Pb date of 2805+\-19 Ma, tentatively interpreted as maximum age for dolerite crystallisation. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv, 100k_geologysub_lut.csv.|2820-2735 Ma (inferred)||Includes Boodanoo Suite, Cullculli Suite, Eelya Suite, Meeline Suite, Mount Kenneth Suite, Rothsay Suite, Warriedar Suite; Edamurta Gabbro.||Amphibole-rich metatonalite, biotite metagranodiorite, dolerite, biotite tonalite gneiss, (meta)monzogranite, gabbro, leucogabbro, gabbronorite, amphibole porphyroblasts, serpentinite, ultramafic schist.|
74813|Annean Supersuite|71270|5|Briefly described|GEOL_LUT_CSV files|||Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. See 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|||Includes Culculli Suite.|||
74813|Annean Supersuite|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|||Warriedar, Cullculli Suites.|||
74813|Annean Supersuite|71272|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|||Boodanoo, Warriedar Suites.|||
74813|Annean Supersuite|71809|5|Briefly described|map legend|Archean|Archean|Yilgarn Craton, Youanmi Terrane|||Includes Boodanoo Suite, Warriedar Suite, Rothsay Suite.|||
74813|Annean Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Mesoarchean|Youanmi Terrane. |||Includes Cullculli Suite and 4 unnamed subunits.||Metagranite, undivided; includes deeply weathered rock. Tonalite, trondjhemite, and granodiorite; metamorphosed. Metaperidotite. Dolerite grading into metadolerite, locally schistose; metamorphosed.|
74813|Annean Supersuite|72389|5|Briefly described|Map Legend|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Gabanintha 1:100k map sheet 2644.|2801-2792 Ma||Includes the Warriedar Suite, Cullculli Suite and the Meeline Suite.|||28-AUG-20
74813|Annean Supersuite|73410|6|Mentioned|p2|||Youanmi Terrane.|2820-2735 Ma.|||||
74813|Annean Supersuite|73596|6|Mentioned|p1168, 1172|Neoarchean|Mesoarchean|Appears as Annean Granite Supersuite on p1172.|2820-2735 Ma.|||||
33445|Antarctic Creek Member|23755|4|Described|p22|Archean|Archean|See also page 22 Fig 9. Of Apex Basalt.||||||07-NOV-08
33445|Antarctic Creek Member|23783|6|Mentioned|p53|||Of Mount Ada Basalt.  Now included as part of the Duffer Formation.||||||
33445|Antarctic Creek Member|64621|5|Briefly described|Map legend|Archean|Archean|Of Mount Ada Basalt (Coongan Subgroup, Warrawoona Group). Arenite and layered black, grey, red and white chert; contains beds with millimetre-size impact spherules; metamorphosed.||||||07-NOV-08
33445|Antarctic Creek Member|64747|6|Mentioned|p120|Paleoarchean|Paleoarchean||3470 +/- 2 Ma (U-Pb zircon: Byerly et al., 2002).|Mount Ada Basalt||||
33445|Antarctic Creek Member|65757|5|Briefly described|p81 Tb.2|Paleoarchean|Paleoarchean|of the Mount Ada Basalt.  Silica-sericite spherules in chert breccia/conglomerate, arenite overlain by jaspilite. Age: 3470.1 +/- 1.9 Ma. [wrongly] Shown as Antarctic Chert Member p82 fig 1.||||||
33445|Antarctic Creek Member|67130|6|Mentioned|p13, p63, p69|Paleoarchean|Paleoarchean|Contains thin layers with sand sized grains of altered quench textured impact spherules.|3470 +/- 2 Ma (U/Pb) |Mount Ada Basalt||Overlain by Duffer Formation, Panorama Formation|Felsic sandstone and layered blue, grey and red chert.|
33445|Antarctic Creek Member|67269|5|Briefly described|p5, p6 Fig.3|Paleoarchean|Paleoarchean|||Mount Ada Basalt.|||Sandstone and chert.|
33445|Antarctic Creek Member|68280|5|Briefly described|p2, p11, p12|Paleoarchean|Paleoarchean||3470 +/- 2 Ma (SHRIMP)|Mount Ada Basalt|||Felsic sandstone, arenites, layered chert with impact generated spherules and spherule bearing chert.|18-JAN-23
33445|Antarctic Creek Member|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Includes 1 unnamed sub-unit.|c. 3470 Ma (Byerly et al. 2002)|Of the Mount Ada Basalt.|||Chert, felsic volcaniclastic rocks, and carbonate rocks, metamorphosed; arenite and layered black, grey, red and white chert, contains an impact spherule bed, metamorphosed.|02-MAY-14
33445|Antarctic Creek Member|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Mount Ada Basalt|||Chert, felsic volcaniclastic rocks, and carbonate rocks; metamorphosed. Arenite and layered chert; metamorphosed.|
33445|Antarctic Creek Member|69563|5|Briefly described|p690 Tb.1|||Contains microkrystite spherules and spherule-bearing conglomerate: asteroid impact ejecta, underlain by a jaspilite unit.|3470.1 +/- 1.9 Ma.|Unit in Mount Ada Basalt.||||
33445|Antarctic Creek Member|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv.|3470 Ma (inferred; isotopic)|Unit of Mount Ada Basalt.|||Arenite and layered black, grey, red and white chert; contains beds with millimetre-size impact spherules; metamorphosed;  felsic volcaniclastic rocks, and carbonate rocks; metamorphosed.|
33445|Antarctic Creek Member|70733|6|Mentioned|p103, 105, 118, 120|||Pilbara Craton; 40km W of Marble Bar. Contains an impact ejecta unit dated at ~3470.1 +/- 1.9 Ma.|~3.47 Ga.|Mount Ada Basalt.||||
33445|Antarctic Creek Member|71267|6|Mentioned|1m_geologyl12_lithology_lut.csv||||||||ash tuff, volcaniclastic rock, chert, arenite|
79992|Anthiby Formation|72712|4|Described|p5,6, p17, p19, p22-25, p29-30, p35.|Siderian|Siderian|New name. Report cover image features this formation. Maximum preserved thickness of 100m in a measured type section. Expected depositional age <c.2340 Ma. Shown as AF on p20 Fig.15f. See also p9, p20, p23-24, p32, p36-37, p42-43, p45, p47, p49.|Max dep age c. 2423 Ma, U-Pb SHRIMP|Top of Turee Creek Group.||Unconformably underlies Beasley Quartzite and unconformably overlies Calgra Member, Kungarra Formation and Munder Formation. Truncates a Balgara Dolerite sill near contact with Calgra Member.|Fine to very fine-grained, cross-stratified sandstone and planar laminated siltstone.|
80953|Antrim Plateau Volcanics and Lally Conglomerate|72034|5|Briefly described|500k_interpgeop16_lut|Series 3|Series 2|Ord Basin, Kalkarindji Large Igneous Province. Informal grouping. Max age inferred. Min age from Antrim Plateau Volcanics.|505+/-2 Ma min age.||||Flood basalts with lesser siliciclastic sedimentary rocks.|
25763|Apex Basalt|23416|5|Briefly described|Map Legend|Archean|Archean|Of Salgash Subgroup, Pilbara Craton||||||07-NOV-08
25763|Apex Basalt|23755|4|Described|p21|Archean|Archean|See also page 17 table 1. Of Warrawoona Group.||||||07-NOV-08
25763|Apex Basalt|23783|5|Briefly described|p12 Tb. 1|||Of Salgash Group.||||||
25763|Apex Basalt|23784|5|Briefly described|p76|Archean|Archean|||||||07-NOV-08
25763|Apex Basalt|23807|6|Mentioned|p110 Fig. 2|||Geological Province: Pilbara Craton.||||||
25763|Apex Basalt|23813|5|Briefly described|p91 Tb. 1|Archean|Archean|Of the Warrawoona Group.  Age: c.3.48-3.43Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.||||||07-NOV-08
25763|Apex Basalt|24025|4|Described|p9 Tb. 1|Archean|Archean|Of Salgash Subgroup (Warrawoona Group).  Tholeiitic pillow basalt, high-Mg basalt, peridotitic komatiite, grey and white layered chert.  Max. thickness: ~2000m.  Geological Province: Pilbara Craton.||||||04-DEC-08
25763|Apex Basalt|24184|5|Briefly described|p699 Fig.3, p701|Archean|Archean|Of the Salgash Subgroup. Underlain by Towers Formation. Geological Province: Pilbara Craton. Max Thickness: 4km. Age: >3459Ma||||||07-NOV-08
25763|Apex Basalt|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group). Carbonate altered basalts, chert. Overlies Towers Formation; overlain by Strelley Pool Chert (??). Age: 3417+/-9Ma. Max. thickness: 2km.See also p130.||||||07-FEB-11
25763|Apex Basalt|31309|2|Defined|p53|Archean|Archean|||||||07-NOV-08
25763|Apex Basalt|38498|5|Briefly described|Table 1|||||||||
25763|Apex Basalt|38544|6|Mentioned|Fig.1|||||||||
25763|Apex Basalt|39672|6|Mentioned|Fig.2|||||||||
25763|Apex Basalt|39697|3|Fully described|p94|||||||||
25763|Apex Basalt|40596|6|Mentioned|Fig.1|||||||||
25763|Apex Basalt|41028|6|Mentioned|p227|||||||||
25763|Apex Basalt|41767|6|Mentioned|p45|||||||||
25763|Apex Basalt|43057|6|Mentioned|Fig.2.7|||of Warrawoona Group||||||
25763|Apex Basalt|43595|6|Mentioned|Table 2-28,p214|||||||||
25763|Apex Basalt|43698|6|Mentioned|p3,5|||||||||
25763|Apex Basalt|43769|6|Mentioned|Fig.3,p858|||||||||
25763|Apex Basalt|44150|5|Briefly described|p129 Tb.2-15,p132 Fig.2-131,p133 Tb.2-16|||See also p139 Tb.2-18, p152 Tb.2-22, p157 Fig.2-144. 1.5 to 2 km thick. Formerly part of Empress Formation (of Fitton et al., 1975) and of Miralga Formation (Ingram, 1977). Indistinguishable from other parts of Warrawoona Group except by its position. Contains microfossils; probably photosynthetic, oxygen-producing cyanobacteria.||Salgash Subgroup||Overlies Towers Formation. Overlain by Panorama Formation.|Metamorphosed pillow basalt and high-Mg basalt; numerous chert units; minor sills of dolerite, gabbro and rarely seen ultramafics .|
25763|Apex Basalt|44229|5|Briefly described|Map Legend|Archean|Archean|Of the Salgash Subgroup.  Mixed, massive and pillowed basalt, high-Mg basalt, and thin intercalated chert.||||||07-NOV-08
25763|Apex Basalt|46922|6|Mentioned|p259|||Trace element analysis.||||||
25763|Apex Basalt|50189|4|Described|p9, 25|Archean|Archean|Lower part of the Salgash Subgroup. Mainly pillowed mafic and ultramafic lavas - with thin beds of chert interlayered with the metabasalts. Disconformably overlies the Duffer Formation. Maximum Thickness: ~2km.||||||07-NOV-08
25763|Apex Basalt|50381|5|Briefly described|Map Legend|Archean|Archean|Of Salgash Subgroup (Warrawoona Group). Geological Province: Pilbara Craton.||||||07-NOV-08
25763|Apex Basalt|50427|5|Briefly described|p194 Fig. 12|Archean|Archean|||||||07-NOV-08
25763|Apex Basalt|50430|4|Described|p160||Archean|Age: 3460-3425 Ma. Up to 4km thick. In East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
25763|Apex Basalt|50544|3|Fully described|p22, p21 Tb. 4|Archean|Archean|Of the Warrawoona Group.  Predominantly pillowed tholeiitic and high-Mg metabasalt.  Disconformably overlies Duffer Formation. Intruded by Coppin Gap and Mullugunya Granodiorites (Mount Edgar Granitoid Complex). Max. thick: ~2000m.||||||18-DEC-12
25763|Apex Basalt|50555|5|Briefly described|Map legend|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group). Mixed massive and pillowed basalt, high-Mg basalt, and thinly intercalated chert.  Geological Province: Pilbara Craton.||||||07-NOV-08
25763|Apex Basalt|60112|5|Briefly described|p108-111.|||||Unit in Warrawoona Group.||Overlies the Duffer Formation.|4km thick, mafic volcanics.|
25763|Apex Basalt|60429|4|Described|p7, p9|Archean|Archean|Lower part of Salgash Subgroup. Disconformable on Duffer Formation. Forms arcuate belt of pillowed mafic + ultramafic lavas.Thickness:~2km; pillowed tholeiitic basalts are fine-grained or amygdaloidal; includes thin beds of blue chert, grey or black chert||||||07-FEB-11
25763|Apex Basalt|60636|6|Mentioned|p55|||Name used interchangeably with Apex Formation.||||||07-FEB-11
25763|Apex Basalt|61111|6|Mentioned|p97 Fig. 3, p108|||Also discussed in relation to cherts from Towers and Apex Basalt Formations.||||||
25763|Apex Basalt|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Geological Province: eastern Pilbara Craton.||||||07-NOV-08
25763|Apex Basalt|61257|5|Briefly described|p345 Fig. 1|Archean|Archean|Ultramafic-mafic volcanics with some chert horizons.  Geological Province: North Pole Dome of the Pilbara Craton.  See also p355 Tb. 1.||||||07-NOV-08
25763|Apex Basalt|61266|5|Briefly described|p58 Tb.1|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group). Carbonate-altered basalts, chert. Geological Province: Pilbara Craton.||||||07-NOV-08
25763|Apex Basalt|61560|5|Briefly described|p498 Tb. 4|Archean|Archean|Includes the Antarctic Chert Member. Contains an impact spherule layer. Geological Province: Pilbara Craton.||||||07-NOV-08
25763|Apex Basalt|61579|5|Briefly described|p58 Fig. 2|Archean|Archean|Of the Warrawoona Group. See also Apex chert which is treated separately in text of study (but which it is understood is cherty horizons within the Apex Basalt).||||||07-NOV-08
25763|Apex Basalt|62427|6|Mentioned|p6 Fig.3, p12, p17  |Paleoarchean|Paleoarchean|Also called Apex Formation, evidently interchangeably.|Between 3459 and <3446 Ma.|||||
25763|Apex Basalt|62979|5|Briefly described|p213|||Of the Warrawoona Group. Ultramafic sequence. Geological Province: Pilbara Craton.||||||07-FEB-11
25763|Apex Basalt|63142|5|Briefly described|p487 Fig. 2|||Geological Province: Warrawoona Syncline.||||||29-MAR-07
25763|Apex Basalt|63245|5|Briefly described|p5 Fig. 2|Archean|Archean|Of the Warrawoona Group. Geological Province: Pilbara Craton.||||||07-NOV-08
25763|Apex Basalt|63417|5|Briefly described|Map legend|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group, Pilbara Supergroup). Geological Province: Pilbara Craton. Basalt, komatiitic basalt, and serpentinised peridotite; local dolerite sills; minor felsic volcaniclastic rocks and chert; metamorphosed.||||||04-DEC-08
25763|Apex Basalt|63420|5|Briefly described|Map legend|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group, Pilbara Supergroup). Geological Province: Pilbara Craton. Basalt, komatiitic basalt and serpentinised peridotite; local dolerite sills; minor felsic volcaniclastic rock and chert; metamorphosed.||||||04-DEC-08
25763|Apex Basalt|63441|5|Briefly described|p4 Tb. 1, p20|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group, Pilbara Supergroup). Overlies Duffer Formation; overlain by Strelley Pool Chert (Kelly Group). Geological province: Pilbara Craton.||||||07-FEB-11
25763|Apex Basalt|63538|4|Described|p3 Fig. 2, p8 Tb. 1, p9, p35, p9 Fig. 3|Archean|Archean|Of Salgash Subgroup (Warrawoona Group). Underlain by Duffer Formation. Geological Province: Pilbara Craton. Weakly to highly vesicular and commonly pillowed basalt.||||||17-APR-13
25763|Apex Basalt|63649|5|Briefly described|p201|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Age: 3.46Ga. Geological Province: Pilbara Craton.||||||07-FEB-11
25763|Apex Basalt|64328|5|Briefly described|p54|||Of the Salgash Subgroup. Basalt.||||||07-FEB-11
25763|Apex Basalt|64405|5|Briefly described|p4 Fig. 3|Archean|Archean|Name inferred from Apex only in Figure 3. Of the Warrawoona Group (De Grey Supergroup). Mount is Mt in text of figure.||||||07-FEB-11
25763|Apex Basalt|64621|5|Briefly described|Map legend|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group, Pilbara Supergroup).||||||07-NOV-08
25763|Apex Basalt|64628|6|Mentioned|p171 Fig.1. |||Coppin Gap greenstone belt, Pilbara Craton.||||||
25763|Apex Basalt|64936|5|Briefly described|map legend|Archean|Archean|Of Salgash Subgroup. Over Marble Bar Chert Member; under Panorama Formation. Basalt, metakomatiite, chert, and conglomerate; weakly metamorphosed. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
25763|Apex Basalt|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton. Mapped as five sub-units.||Of Salgash Subgroup.||Intrudes Duffer Formation and Mount Edgar Granitoid Complex.|Massive and pillowed tholeiitic basalt, komatiitic basalt, and thin intercalated chert, metamorphosed; mafic and ultramafic schist; serpentinite; banded chert; fuchsitic quartzite; dolerite dykes and pods.|
25763|Apex Basalt|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Mapped as six sub-units.||Of Salgash Subgroup.|||Basalt, komatiitic basalt, local talc-carbonate rock, chert, metamorphosed; mafic and ultramafic schist; serpentinite; banded chert; fuchsitic quartzite; dolerite sills, dykes and pods; local banded iron formation.|
25763|Apex Basalt|65757|6|Mentioned|p82 Fig.1, p87|Paleoarchaen|Paleoarchean|[Wrongly] said to include the Antarctic Chert Member [misspelling of Antarctic Creek Member]. Age [of Antarctic Creek Member]: 3470.1+/-1.9 Ma. In the North Pole Dome, Pilbara Craton. Of Warrawoona Group.||||||06-OCT-15
25763|Apex Basalt|65827|3|Fully described|p12 Tb.3,p18-19,p22-25,p33,p40-41,p46|Paleoarchean|Paleoarchean|Of Salgash Subgroup. c.3458-3410 Ma. Over 2 km thick. Intruded by Zulu, Chessman, Wilina, Kennell, Mullugunya and Chimingadgi Granodiorites, Walgunya Trondhjemite. Intrudes Underwood and Fig Tree Gneisses, and Duffer Formation. Underlies Panorama Fm; unconformably underlies Fortescue Group; unconformably overlies Duffer Fm, Mount Roe Basalt. Massive, fine-grained, locally pillowed tholeiitic basalt which has undergone widespread shearing; local basal chert are rare BIF. Hosts the high-grade Invincible gold mine.||||||
25763|Apex Basalt|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Salgash Subgroup. Basalt, komatiitic basalt, serpentinized peridotite; local dolerite sills; minor felsic volcaniclastic rocks and chert; metamorphosed. Includes unnamed talc-carbonate unit derived from metaperidotite, with volcanic protoliths.||||||
25763|Apex Basalt|66217|4|Described|p5, p8, p14, p15, pp24-27, p60.|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Of Hickman (1977); Van Kranendonk et al. (2002) included this unit in the Salgash Subgroup in their redefinition of the Warrawoona Group. Stratiform Cu-Zn mineralisation locally present in pelitic schist. Thickness to 3250 m.||Lower unit in Salgash Subgroup.||Feeder dykes intrude Duffer Formation, Callina Supersuite, Mount Ada Basalt and Talga Talga Subgroup. Is conformably overlain by Panorama Formation.|Low-grade, dominantly pillowed, basalt; pyroxene spinifex-textured komatiitic basalt; peridotitic komatiite; thin horizons of chert, black shale, and felsic volcaniclastic rocks.|18-DEC-12
25763|Apex Basalt|66664|6|Mentioned|p9.|||||Unit in Warrawoona Group.|||Komatiitic pillow basalt; minor chert.|
25763|Apex Basalt|66745|4|Described|p53 Fig.3, p54 Fig.4.|Paleoarchean|Paleoarchean|Major deepening of depositional basins, with many kilometres of deep-water volcanic rocks.||Unit in Salgash Subgroup.||Disconformably overlies Duffer Formation. Is overlain by Panorama Formation.|Komatiite, komatiitic basalt, basalt; thin units of chert.|
25763|Apex Basalt|67130|6|Mentioned|p15 fig 10, p20 fig 13, p55, p58|||Up to 3km thick.||Warrawoona Group||Overlies Marble Bar Chert Member, overlain by Panorama Formation|Basalt and ultramafic lavas, bedded chert.|
25763|Apex Basalt|67197|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Salgash Subgroup.||||
25763|Apex Basalt|67201|4|Described|p7 Fig.4, p12 Tb.1, p24|||In northern Pilbara Craton, East Pilbara Terrane.||Salgash Subgroup||||
25763|Apex Basalt|67269|5|Briefly described|p8, p13|Paleoarchean|Paleoarchean|Generally 3-4 km thick. Entirely removed by erosion in the Panorama greenstone belt.|3460-3450 Ma.|Salgash Subgroup.||Overlies Marble Bar Chert Member (Duffer Formation). Is overlain by Panorama Formation.||
25763|Apex Basalt|67270|4|Described|p1-2, p4-6, p10-15, p17-18, p21-22|Paleoarchean|Paleoarchean|Hickman (1977). Near Marble Bar. 3-4 km thick. Cross-cut by hydrothermal silica "chert" veins. Lithology detailed. Photographs, photomicrographs.|3460-3450 Ma.|Salgash Subgroup.|"Apex chert".||Mainly basalt, much of which is spinifex-textured komatiitic basalt. Includes a stratiform unit of bedded grey to black chert, with associated mafic-felsic volcaniclastic rocks. Ferruginous cherts are crosscut by black-and-white chert.|
25763|Apex Basalt|67668|5|Briefly described|Fig. 2-4; p153-4, 156, 161, 163; Tb.1. ||Paleoarchean|East Pilbara Terrane, Pilbara Craton. Controversial evidence of early life is reviewed. |ca 3460 Ma|Warrawoona Group||Underlies the Panorama Formation, overlies the Marble Bar Chert.|Mafic volcanic rocks.|
25763|Apex Basalt|68035|4|Described|p293, p288 Fig 4|Paleoarchean|Paleoarchean|Warrawoona Group, Pilbara Supergroup, East Pilbara Terrane.|3.46-3.45 Ga|Of Salgash Subgroup.||Disconformably overlies Duffer Formation. Overlain by Panorama Formation.|Komatiite, komatiitic basalt,basalt.|
25763|Apex Basalt|68280|5|Briefly described|p4, p30, p32|||Includes five unnamed (Apex Chert is an informal name) laterally persistent chert units, with possible microfossils present throughout (currently controversial). Apex chert is 25m thick and consists of silicified volcaniclastic tuffs interlayered with chert and overlying a pebble to cobble conglomerate.||||Overlain by Panorama Formation|Pillow basalt, komatiitic basalt and komatiite, hyaloclastite, fossiliferous chert.|
25763|Apex Basalt|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Salgash Subgroup.|||Metachert; blue-grey and white chert (recrystallised); amphibolite schist derived from metabasalt.|23-SEP-13
25763|Apex Basalt|68282|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. 11 facies are mapped separately.||Of the Salgash Subgroup|||Metamorphosed basalts: komatiitic and tholeiitic; talc-, serpentine-, mafic-, chlorite-actinolite- schists; interlayered amphibolite and granitic rocks, commonly schistose; metachert; white, medium-grained quartzite.|12-JUN-14
25763|Apex Basalt|68283|5|Briefly described|Map Legend|Archean|Archean|East Pilbara Terrane, Pilbara Craton. Includes 1 unnamed subunit.||Of the Salgash Subgroup.|||Basalt, komatiitic basalt, and serpentinized peridotite, local dolerite sills, minor felsic volcaniclastic rock and chert; white, grey, and blue-black layered chert, locally massive blue-grey; all metamorphosed.|23-SEP-13
25763|Apex Basalt|68284|5|Briefly described|p2, 4-5, 7, 20|Paleoarchean|Paleoarchean|Pilbara region. The Schopf State Geoheritage Reserve R48969 occurs in this unit; a microfossil locality.|3460-3450 Ma.|Salgash Subgroup (Warrawoona Group).||Overlies Marble Bar Chert Member (Duffer Formation); Dresser Formation. Is overlain by Panorama Formation. Is intruded by Corunna Downs Granitic Complex.|Contains a chert unit with probable microfossils.|
25763|Apex Basalt|69012|6|Mentioned|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane. The four facies are mapped separately.||Of the Salgash Subgroup.|||Metamorphosed pillowed and massive basalt; metamorphosed bedded to massive quartz-rich sandstone; amphibolite and amphibolitic schist; strongly sheared chloritic schist after metabasalt.|28-APR-14
25763|Apex Basalt|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Salgash Subgroup.|||Carbonate-altered mafic volcanic rock and derived mafic schist.|02-MAY-14
25763|Apex Basalt|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Metadolerite, silicified metabasalt, mafic/ultramafic schist, Silicified shale, sandstone, felsic volcaniclastic sandstone, rhyolite flows and felsic tuffaceous rocks, dunite, pyoxene peridotite, pyroxenite.||Salgash Subgroup|||Basalt, komatiitic basalt, serpentinized peridotite, serpentinite and conglomerate. Pelite, quartzite, metachert, amphibolite and amphibolitic schist. talc/serpentine schist, chloritic schist, amphibolite schist, metakomatiitic basalt.|
25763|Apex Basalt|69301|4|Described|p5 Fig.3, p9 Tb.1, p10-11, p20 Tb.2|||Pilbara Craton. East Pilbara Terrane.||Salgash Subgroup||Disconformity at base.|Basalt, komatiitic basalt, komatiite|
25763|Apex Basalt|69566|6|Mentioned|p236|||East Pilbara Granite-Greenstone Terrane.||Warrawoona Group.||Overlies Duffer Formation. Is overlain by Panorama Formation.||
25763|Apex Basalt|69569|6|Mentioned|p284-285, 287-288|||Marble Bar greenstone belt, East Pilbara Terrane.||Warrawoona Group.|Apex chert.||Pillow basalt and komatiite, green-grey volcaniclastics and lavas, stratiform chert, pyroclastic breccia, green tuff, grey tuff.|
25763|Apex Basalt|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 250k_interpgeol_lut.csv.|3460-3449 Ma (inferred)|Unit of Salgash Subgroup.|||Amphibolite, basalt, sandstone, chert, conglomerate, dunite, volcaniclastic sandstone, schist, komatiite, peridotite, pyroxenite, rhyolite, serpentinite; variably interlayered, silicified, metamorphosed.|
25763|Apex Basalt|69989|6|Mentioned|p26|Paleoarchean|Paleoarchean|North Pole Dome area, Pilbara Craton.|3.46 Ga.|Warrawoona Group.||Overlies Marble Bar Chert. Is overlain by Panorama Formation.||
25763|Apex Basalt|70022|6|Mentioned|p115|||East Pilbara Terrane.||Salgash Subgroup.||||
25763|Apex Basalt|70729|4|Described|p161-163,165,173|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Best exposed in the Marble bar greenstone belt, approximate thickness ~3km. Underwent metamorphism up to prehnite-pumpellyite to lower greenschist facies (Hickman and Lipple, 1978; Van Kranendonk et al., 2007). Includes at least 5 stratiform chert units; concordant, bedding parallel units that are often internally laminated and preserve sedimentary structures (Kato and Nakamura, 2003; Brasier et al., 2011). Intruded by series of hydrothermal black chert veins cut up through the lower portions of the Apex Basalt for up to 1600 m. |c. 3.53-3.43 Ga|Unit of Warrawoona Group.|Includes Apex chert.|Underlain by Marble Bar Chert/Duffer Formation.|Extrusive volcanic rocks with minor interstratified chert, barite, carbonate and volcaniclastic units.|
25763|Apex Basalt|70733|6|Mentioned|p103-107|||Pilbara Craton.|3459-3449 Ma.|||Overlies Duffer Formation. Is overlain by Panorama Formation. Overlies and intrudes Marble Bar Chert Member.|Basalt; dolerite sills and feeder dykes; local chert.|
25763|Apex Basalt|70775|5|Briefly described|p12|||East Pilbara.||Warrawoona Group||Overlies the Duffer Formation. Overlain by the Panorama Formation.||
25763|Apex Basalt|70834|5|Briefly described|p297-298|||Marble Bar area, East Pilbara granite greenstone terrane, Pilbara Craton.|c.3.46 Ga.|Warrawoona Group.||Overlies Marble Bar Chert. Is overlain by Panorama Formation. Is intruded by Apex chert veins.|Basalt, komatiite, felsic volcanics, chert.|
25763|Apex Basalt|70884|5|Briefly described|p123-124|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Salgash Subgroup.||Overlain by Panorama Formation. Underlain by Marble Bar Chert Member/Coongan Subgroup.||
25763|Apex Basalt|71487|6|Mentioned|p130|||Geological province: Pilbara Craton.||||||
25763|Apex Basalt|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Warrawoona  Large Igneous Province.||Salgash Subgroup|||Basalt, komatiitic basalt, serpentinized peridotite; local dolerite sills; minor felsic volcaniclastic rocks and chert; metamorphosed.|
25763|Apex Basalt|72064|5|Briefly described|p66|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawoona Group.||Overlain by Panorama Formation. Underlain unconformably by Duffer Formation.||
25763|Apex Basalt|72251|5|Briefly described|p54-55|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Salgah Subgroup.||Overlain by Panorama Formation. Underlain by Duffer Formation.||
25763|Apex Basalt|72668|6|Mentioned|p4-6, p17, p19|||East Pilbara Terrane. Said to be fed by a mafic dyke swarm. Up to 4 km thick in some areas.||Salgash Subgroup||Overlain by the Panorama Formation.||12-JAN-22
25763|Apex Basalt|73598|6|Mentioned|p1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Salgash Subgroup.||Overlies Duffer Formation. Is overlain by Panorama Formation.||
74208|Aquitaine Formation|61542|5|Briefly described|p277 Fig. 2|Namurian|Namurian|Of the Wadeye Group - offshore equivalent of the onshore Point Spring Sandstone. Geological Province: onshore Bonapart Basin/Petrel-Sub-basin. Lower sandstone grading up into siltstone.||||||07-FEB-11
74208|Aquitaine Formation|67354|6|Mentioned|p73. |||||Offshore unit in Wadeye Sub-Group.||||
74208|Aquitaine Formation|69452|3|Fully described|p36:9, 15, 17|||Gorter et al. (2005). Subsurface. Petrel Sub-basin, Bonaparte Basin. Is 95m thick in the type section in Sandbar-1. Mostly non-marine deposits. Over 200m thick. Offshore and onshore.||Wadeye Group.||Unconformably overlies Arco Formation. Lateral equivalent of Point Spring Sandstone (WA). Is overlain unconformably by Kuriyippi Formation.|Fine- to coarse-grained sandstone with a few siltstone interbeds, grading up into siltstone.|12-JUL-16
74208|Aquitaine Formation|69653|6|Mentioned|p10|Carboniferous|Carboniferous|Petrel Sub-basin.||Wadeye Group.||Overlies Arco Formation. Is overlain by Kuriyippi Formation (Kulshill Group).||
74208|Aquitaine Formation|69673|5|Briefly described|p172|||||Wadeye Group|||Interbedded siltstone/shale and sandstone.|
74208|Aquitaine Formation|70061|5|Briefly described|Petrel Sub-basin Figs.2 & 3, p3|Bashkirian|Bashkirian|See also Regional geology: Fig.8. Hydrocarbon reservoir.||Wadeye Group.||Overlies Arco Formation. Is overlain by Kuriyippi Formation.||12-JUL-16
74208|Aquitaine Formation|73117|6|Mentioned|p15|Bashkirian|Bashkirian|Bonaparte Basin, southern. Palynozonation: S. ybertii.||Wadeye Group||Underlain by Arco Formation. Equivalent to Point spring Sandstone.||
74209|Arco Formation|61542|4|Described|p277 Fig. 2, p288|Namurian|Namurian|Offshore equiv.of onshore Point Spring Sst. Variously overlies Sunbird and Tanmurra Fms.+ Kingfisher Shale.  Geol.P:onshore Bonapart Basin/Petrel-Sub-basin.Interbedded  pyritic siltstone fine- to coarse-gr.sandstones; occasional fossils.||||||07-FEB-11
74209|Arco Formation|67354|6|Mentioned|p73. |||||Offshore unit in Wadeye Sub-Group.||||
74209|Arco Formation|69452|3|Fully described|p36:9, 15, 17|||Gorter et al. (2005). Subsurface. Petrel Sub-basin, Bonaparte Basin. The type section is in the offshore drillhole Sandbar-1, where it is 105m thick (see Lithology). Shallow marine deposits. Up to 650m thick. Offshore and onshore.||Wadeye Group.||Unconformably overlies Sunbird or Tanmurra Formations. Lateral equivalent of Point Spring Sandstone (WA). Is overlain unconformably by Aquitaine Formation.|Lower 62m-thick interval of interbedded siltstone and fine- to very coarse-grained sandstone; up to 5% recrystallised limestone grains, occcasional fossils and common calcite cement; below fine- to coarse- and rarely very coarse-grained sandstone.|12-JUL-16
74209|Arco Formation|69653|6|Mentioned|p10|Carboniferous|Carboniferous|Petrel Sub-basin.||Wadeye Group.||Overlies Sunbird Formation (Weaber Group). Is overlain by Aquitaine Formation.||
74209|Arco Formation|69673|5|Briefly described|p172|Pennsylvanian|Serpukhovian|Age derived from fossils.||Wadeye Group|||Interbedded siltstone/shale and sandstone.|
74209|Arco Formation|70061|5|Briefly described|Petrel Sub-basin Figs.2 & 3, p3|Bashkirian|Bashkirian|See also Regional geology: Fig.8, p11. Hydrocarbon reservoir.||Wadeye Group.||Is overlain by Aquitaine Formation.||12-JUL-16
74209|Arco Formation|73117|6|Mentioned|p15|Serpukhovian|Serpukhovian|Bonaparte Basin, southern. Palynozonation: S. ybertii.||Wadeye Group||Overlain by Aquitaine Formation. Equivalent to Point spring Sandstone.||
75379|Argus Igneous Complex|66119|5|Briefly described|Map legend|Archean|Archean|Yamarna Terrane, Yilgarn Craton. Age shown as c.2737 Ma. Metamorphosed anorthosite; contains interleaved amphibolite.||||||
75379|Argus Igneous Complex|66121|5|Briefly described|Map legend|Archean|Archean|Yamarna Terrane, Yilgarn Craton. Metamorphosed anorthosite (c.2737 Ma) with interleaved amphibolite and talc-serpentine-chlorite schist; amphibolite, medium- to coarse-grained, derived from gabbro, interleaved with talc-serpentine-chlorite schist.||||||
75379|Argus Igneous Complex|68107|5|Briefly described|p607 Fig.3, p609 Tb.1, p610, p617.|Neoarchean|Neoarchean|Mount Venn Greenstone Belt, Burtville Terrane.|2737 +/- 26 Ma (Wingate et al. 2011g).||||Small, deformed, layered anorthosite and gabbro sill.|
75379|Argus Igneous Complex|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yamarna Terrane, Eastern Goldfields Superterrane, Yilgarn Craton|||Includes 2 unnamed subunits.||Amphibolite; medium- to coarse-grained, derived from gabbro; fine- to coarse-grained meta-anorthosite; minor interleaved amphibolite and talc-serpentine-chlorite schist.|05-AUG-15
75379|Argus Igneous Complex|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|See also 100k_geologyp14_lut.csv. Age derived from metamorphosed anorthosite sample (185970.1.pdf).|2737 +/- 26 Ma (isotopic).||||Amphibolite; medium to coarse grained, derived from gabbro; locally interleaved talc-serpentine-chlorite schist. Strongly foliated, fine- to coarse-grained meta-anorthosite; minor interleaved amphibolite and talc-serpentine-chlorite schist.|
75379|Argus Igneous Complex|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||||||Amphibolite derived from gabbro and meta-anorthosite, and locally interleaved talc-serpentine-chlorite schist.|
75379|Argus Igneous Complex|73596|6|Mentioned|p1170|Neoarchean|Neoarchean|Mount Venn Greenstone Belt, Burtville Terrane.|2737 +/- 26 Ma.|||||
80989|Arid Basin unit|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Arid Basin. |||||Psammitic and semipelitic gneiss, locally garnet-rich; interlayered with mafic amphibolite to granulite and granitic gneiss.|
36759|Aries kimberlite|23772|5|Briefly described|p763|||In the Kimberley Block. Not intended as a formal name.||||||18-JUL-06
36759|Aries kimberlite|62715|5|Briefly described|p1752, p1779|Neoproterozoic|Neoproterozoic|Intrudes the Kimberley Group.  Geological Province: Kimberley Basin. See also Aries micaceous kimberlite.||||||04-OCT-06
36759|Aries kimberlite|69585|6|Mentioned|p30|||Central Kimberley Basin. A granite xenolith has an age and whole-rock Nd isotope character consistent with granites of the Paperbark Supersuite, suggesting a Palaeoproterozoic domain beneath the Basin.||||||
36759|Aries kimberlite|69597|6|Mentioned|p3, p5 fig 2b|||||||||
31793|Armanda intrusion|43854|5|Briefly described|Map Legend||Proterozoic|||||||
31793|Armanda intrusion|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31793|Armanda intrusion|60498|6|Mentioned|p1019-1020.|Paleoproterozoic|Paleoproterozoic|No lithology was stated for the stratigraphic name. Electron microprobe geochemical analyses of apatites are detailed.||||||
31793|Armanda intrusion|63866|5|Briefly described|p131|Orosirian|Orosirian|Central Zone, Halls Creek Orogen.|c. 1845-1830 Ma||||Ultramafic-mafic plutonic rocks.|
31793|Armanda intrusion|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Layered mafic-ultramafic intrusions; peridotite, troctolite, gabbro, olivine gabbro, gabbronorite, magnetite gabbro, magnetite-olivine gabbro, leucogabbro, leucogabbronorite, and anorthosite.||||||
31793|Armanda intrusion|69099|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|Grouped as McIntosh, Armanda, and Spring Creek intrusions, with single lith description in 500k_geologyp08_lut.csv. |||||layered mafic-ultramafic intrusions; peridotite, troctolite, gabbro, olivine gabbro, gabbronorite, magnetite gabbro, magnetite-olivine gabbro, leucogabbro, leucogabbronorite, and anorthosite.|
31793|Armanda intrusion|71113|6|Mentioned|p96|||Geological province: Central Zone, Lamboo Province, Halls Creek Orogen.||||||
31793|Armanda intrusion|71267|4|Described|GEOL_LUT_CSV files|||See 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|||||Layered mafic-ultramafic intrusion; gabbro, leucogabbro, leucogabbronorite, gabbronorite, anorthosite, minor troctolite; some olivine and/or chromitite-bearing; in rhythmic cycles; peridotite and troctolite|
25765|Arrino Siltstone|36293|2|Defined|p54|Proterozoic|Proterozoic|||||||
25765|Arrino Siltstone|36872|3|Fully described|p73|||||||||
25765|Arrino Siltstone|37460|6|Mentioned|p178|||||||||
25765|Arrino Siltstone|40307|6|Mentioned|Fig.2|||||||||
25765|Arrino Siltstone|40346|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25765|Arrino Siltstone|40347|6|Mentioned|p15|||||||||
25765|Arrino Siltstone|41271|6|Mentioned|p228|||||||||
34563|Ashbrook Sandstone|12758|5|Briefly described|p13, p3 Fig. 3|Early Permian|Early Permian|Of the Sue Group.  Conformably overlain by Redgate Coal Measures; conformably overlies Rosabrook Coal Measures.   Max. thickness: 262m (only 135m thick in type section).  Geological Province: Southern Perth Basin.  See also p8 Fig.9.||||||20-OCT-04
34563|Ashbrook Sandstone|22818|5|Briefly described|map|Late Permian|Early Permian|Sue Group||||||
34563|Ashbrook Sandstone|22819|5|Briefly described|map|Early Permian|Late Permian|Sue Group||||||
34563|Ashbrook Sandstone|22820|2|Defined|p8-9 Tbs. 1&2, p18|Early Permian|Early Permian|Of Sue Group. Max. thickness: 200m. Geol.prov: south Perth Basin. Numerous upward-fining cycles dominated by sandstone. Detailed lithology given.||||||29-APR-09
34563|Ashbrook Sandstone|24443|5|Briefly described|Fig.31|Early Permian|Early Permian|Of Sue Group. Conformably overlies Rosabrook Coal Measures. Conformably overlain by Redgate Coal Measures. Geological Province: Perth Basin.||||||
34563|Ashbrook Sandstone|50107|5|Briefly described|Map legend|Permian|Permian|Of the Sue Group.  Geological Province: Southern Perth Basin.||||||
34563|Ashbrook Sandstone|60386|5|Briefly described|p311|||Southern Perth Basin. Non-marine.||||||
34563|Ashbrook Sandstone|64630|5|Briefly described|p31 Fig.2|Artinskian|Artinskian|Province: Southern Perth Basin. Overlies the Rosabrook Coal Measures, underlies the Redgate Coal Measures. Palynology age: M. trisina. Middle correlates with middle of Ewington Coal Measures.||||||
34563|Ashbrook Sandstone|67925|4|Described|Ch2 p10 fig 4, Ch2 p11-p12|Kungurian|Artinskian|A type section in the Sue 1 drillhole is said to be 262m thick. Interpreted to have been deposited in a lacustrine-deltaic environment. Palynology discussed. See also Ch2 p20, Ch2 p26-p28, Ch2 p30, Ch3 p8, Ch4 p8 fig 2.||Sue Group||Overlies the Rosabrook Coal Measures. Conformably overlain by the Redgate Coal Measures.|Poorly sorted feldspathic sandstone.|
34563|Ashbrook Sandstone|69029|6|Mentioned|p332|Kungurian|Artinskian|Of Perth Basin.||||Overlain by Carynginia Formation. Underlain by Irwin River Coal Measures.||
34563|Ashbrook Sandstone|69081|5|Briefly described|p737 Fig.1|Cisuralian|Cisuralian|Presented as Ashbrook Sst in figure. Geol. Prov: Perth Basin||Sue Group||is overlain by Redgate Coal Measures; overlies Rosabrook Coal Measures||
34563|Ashbrook Sandstone|69182|6|Mentioned|Ch2 p9, Ch2 p45, Ch2 p47-p49|Early Permian|Early Permian|Perth Basin. See also  Ch2 p55, Ch2 p57, Ch2 p60, Ch2 p64-p66, Ch2 p80, Ch2 p84, Ch2 p91, Ch2 p92, Ch2 p94-p96, Ch2 p98, Ch2 p100, Ch2 p102, Ch2 p104, Ch2 p106, Ch2 p108, Ch2 p110.||Sue Group||Overlies the Rosabrook Coal Measures. Overlain by the Redgate Coal Measures.||
34563|Ashbrook Sandstone|69297|6|Mentioned|p175, p189|Roadian|Kungurian|Vlaming Sub-basin, South Perth Basin. ||Sue Group||Overlies the Rosabrook Coal Measures. Overlain by the Redgate Coal Measures.||
34563|Ashbrook Sandstone|70097|5|Briefly described|p2, p19 Fig.3|Kungurian|Artinskian|Southern Perth Basin. Bunbury Trough.||Sue Group|||Deglaciation, deltaic sediments. Sandstone.|
34563|Ashbrook Sandstone|70099|5|Briefly described|Fig.4|Kungurian|Kungurian|||Sue Group.||Overlies Rosabrook Coal Measures. Is overlain by Redgate Coal Measures.||
34563|Ashbrook Sandstone|70128|5|Briefly described|p449|Permian|Permian|Southern Perth Basin.||Sue Group.||Conformably overlies Rosabrook Coal Measures. Is overlain conformably by Redgate Coal Measures.||
34563|Ashbrook Sandstone|70774|5|Briefly described|p5 fig 3|Artinskian|Artinskian|Southern Perth Basin.||||Overlies the Rosabrook Coal Measures. Overlain by the Redgate Coal Measures.||
34563|Ashbrook Sandstone|71146|5|Briefly described|p6|Guadalupian|Guadalupian|Perth Basin.||||Overlies the Rosabrook Coal Measures. Overlain by the Redgate Coal Measures.|Sandstone.|
34563|Ashbrook Sandstone|71377|5|Briefly described|p7|Permian|Permian|Perth Basin.||Stockton Group||||
34563|Ashbrook Sandstone|72258|5|Briefly described|p129|Cisuralian|Cisuralian|Of Perth Basin.||||Overlain by Redgate Coal Measures. Underlain by Rosabrook Coal Measures. Laterally grades into Irwin River Coal Measures.||
77087|Athena Basalt|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2680 Ma (inferred).|Great Boulder Suite|||Tholeiitic basalt, massive to pillowed; metamorphosed.|
77087|Athena Basalt|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2680 Ma (inferred)|Unit of Great Boulder Suite.|||Tholeiitic basalt, massive to pillowed; metamorphosed|
77087|Athena Basalt|72252|6|Mentioned|p11|||St. Ives Au-Ni camp, Kambalda Domain, Yilgarn Craton. Up to 300m thick.|||||Pillow or aphyric basalt.|
74823|Atley Igneous Complex|44149|6|Mentioned|p120 Fig.2-125|||Appears as Atley Complex.||||||
74823|Atley Igneous Complex|64891|5|Briefly described|p37 Fig. 2, p50-51 Tb. 1|Archean|Archean|Of the Meeline Suite. Age: c. 2780Ma. Geological province: Murchison Domain. Layered gabbro and anorthosite, with magnetite and pyroxenite layers; metamorphosed.||||||07-FEB-11
74823|Atley Igneous Complex|66195|4|Described|p604, p598 Fig.1, p599 Fig.2, p600, 602|Neoarchean||||In Meeline Suite.|||Main zone: gabbronorite and leucocratic magnetitite and leucogabbro and leucocratic gabbronorite (~1km thick). Upper zone: leucocratic magnetitite and leucogabbro and leucocratic anorthosite (~200m thick).|13-MAR-12
74823|Atley Igneous Complex|67129|5|Briefly described|p18 Fig.19, p52, p54, p56, p57 Fig.61|Archean|Archean|Murchison Domain, Youanmi Terrane.|c.2810 Ma.|Meeline Suite.||||06-SEP-17
74823|Atley Igneous Complex|68519|5|Briefly described|Map Legend|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Of the Meeline Suite.|||Metagabbro, magnetitite, gabbro, serpentinite, dolerite, leucogabbro; all metamorphosed.|
74823|Atley Igneous Complex|68561|5|Briefly described|GEOCHRON files|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane. See geochron file 194747.1.pdf.||Meeline Suite||||
74823|Atley Igneous Complex|69583|4|Described|p49-50, p55-56, p98-102, p177; Plate 2|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Mineralisation style, geochronological data, igneous stratigraphic column. Possibly once part of the Windimurra Igneous Complex.|c.2810 Ma.|Meeline Suite.|||Tremolite schist derived from intrusive rock; gabbro with well-developed modal layering; magnetitite units interlayered with gabbro; layered gabbro, serpentinite derived from peridotitic igneous layers. Metamorphosed.|
74823|Atley Igneous Complex|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean|||Meeline Suite||||
74823|Atley Igneous Complex|69586|5|Briefly described|p22|Mesoarchean|Mesoarchean|Murchison Domain.||Meeline Suite.||||
74823|Atley Igneous Complex|70419|5|Briefly described|p7-9|||Between 3 to 5 km thick; has distinctive magnetitite units in its upper zone. Possibly could have been part of the Windimurra Igneous Complex, now separated by 12-32 km width of granitic plutons.||Meeline Suite.||||
74823|Atley Igneous Complex|70796|5|Briefly described|100k_interpgeop_lut.csv|Mesoarchean|Mesoarchean|Yilgarn Craton. See also 500k_interpgeop14_lut.csv, 194751.1.pdf, Windimurra100_2641_stratig.pdf.|ca 2813 Ma (inferred)|||||
74823|Atley Igneous Complex|70830|5|Briefly described|p4, p27, p31|||||Meeline Suite||||
74823|Atley Igneous Complex|71168|5|Briefly described|p7|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c. 2800 Ma|Meeline Suite||||
74823|Atley Igneous Complex|71311|6|Mentioned|p794|||Northern Youanmi Terrane, Yilgarn Craton.||||||
74823|Atley Igneous Complex|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Youanmi Terrane. Informally subdivided into 6 unnamed units, 2 upper zone, 2 middle zone and 2 general lithologically based units.|||||Gabbro with well developed modal layering of pyroxene and plagioclase; locally grading into leucogabbro and gabbronorite; metamorphosed. Tremolite schist derived from intrusive rock.|
80991|Atley Igneous Complex, middle zone|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Youanmi Terrane.||Atley Igneous Complex|||Gabbro with well developed modal layering of pyroxene and plagioclase; locally grading into leucogabbro and magnetite-bearing gabbro; metamorphosed. Serpentinite derived from peridotitic igneous layers; locally grades into metapyroxenite.|
80992|Atley Igneous Complex, upper zone|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Youanmi Terrane.||Atley Igneous Complex|||Magnetitite units interlayered with magnetite- and ilmenite-bearing leucogabbro; modally layered on a metre scale; metamorphosed. Gabbro grading into magnetite- and ilmenite-bearing olivine gabbro, leucogabbro and gabbronorite; metamorphosed.|
74824|Austin Downs Supersuite|64891|5|Briefly described|p37 Fig. 2, p42, p50-51 Tb. 1|Archean|Archean|Contains the Big Bell and Yalgowra Suites. Age: 2719-~2694Ma. Geological province: Murchison Domain. Monzogranite, layered gabbro sills, and dolerite; commonly foliated; metamorphosed.||||||07-FEB-11
74824|Austin Downs Supersuite|65548|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Youanmi Terrane, Yilgarn Craton. Includes Yalgowra Suite with the Gnannagooragoo Igneous Complex.||||||02-MAY-16
74824|Austin Downs Supersuite|65550|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Murchison Domain, Youanmi Terrane. Includes Yalgowra Suite. ||||||
74824|Austin Downs Supersuite|66195|5|Briefly described|p599 Fig.2|Neoarchean||Contains Big Bell Suite.||||||13-MAR-12
74824|Austin Downs Supersuite|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|age range at least 2735-2702 Ma||Includes Yalgowra and Big Bell Suites.|||02-MAY-16
74824|Austin Downs Supersuite|67129|6|Mentioned|p18 fig 19|Archean|Archean|Murchison Domain, Youanmi Terrane.|2735-2690 Ma.||Big Bell, Yalgowra Suites.|||06-SEP-17
74824|Austin Downs Supersuite|68107|6|Mentioned|p618|Neoarchean|Neoarchean|Western Youanmi Terrane.|ca. 2716-2694 Ma|||||
74824|Austin Downs Supersuite|68561|5|Briefly described|GEOL_LUT_CSV folder + GEOCHRON files||||||Includes Big Bell Suite, Yalgowra Suite.|||
74824|Austin Downs Supersuite|68698|5|Briefly described|p4-5, p14|Neoarchean|Neoarchean|REE plots.|c.2794 Ma to c.2690 Ma.||Big Bell, Yalgowra Suites.||Includes foliated tonalitic to monzogranitic rocks.|
74824|Austin Downs Supersuite|69014|6|Mentioned|Map Legend|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane.|||Includes the Big Bell Suite.|||
74824|Austin Downs Supersuite|69583|5|Briefly described|p49, p51; Plate 2|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. The felsic intrusives of this unit are assigned to the Big Bell Suite.|||Yalgowra, Big Bell Suites.|||
74824|Austin Downs Supersuite|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean||||Big Bell Suite|||
74824|Austin Downs Supersuite|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.|||Big Bell Suite.|||
74824|Austin Downs Supersuite|69627|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton|||Big Bell Suite, Yalgowra Suite|||
74824|Austin Downs Supersuite|69628|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton|||Big Bell Suite|||
74824|Austin Downs Supersuite|69744|6|Mentioned|p254, 259|||Mount Magnet Greenstone Belt.|2735-2690 Ma.|||||
74824|Austin Downs Supersuite|70020|5|Briefly described|p118|Neoarchean|Neoarchean|Geological province: Yilgarn Craton.|||Includes Big Bell Suite.|Overlain by Tuckanarra Suite. Underlain by Eelya Suite/Annean Supersuite.||
74824|Austin Downs Supersuite|70030|5|Briefly described|p192|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton.|2753-2690 Ma||Includes Big Bell Suite.|||
74824|Austin Downs Supersuite|70139|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Appears also as Austin Down Supersuite.|||Yalgowra, Big Bell Suites.||Peridotite, gabbro, dolerite, quartz gabbro and gabbronorite; monzogranites; all metamorphosed and foliated to a greater or lesser degree.|
74824|Austin Downs Supersuite|70153|6|Mentioned|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean||||Includes Big Bell Suite.|||
74824|Austin Downs Supersuite|70156|5|Briefly described|500k_interpgeop14_lut.csv|||Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton.|||Includes Big Bell Suite.|||
74824|Austin Downs Supersuite|70226|5|Briefly described|Map legend.|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Carton.|||Big Bell Suite|||16-DEC-15
74824|Austin Downs Supersuite|70418|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Appears on the main legend as Austin Down Supersuite.|2735-2690 Ma.||Yalgowra, Big Ben Suites.|||
74824|Austin Downs Supersuite|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton. Also appears as Austin Down Supersuite.|c.2735-2690 Ma.||Big Bell Suite.|||03-MAR-17
74824|Austin Downs Supersuite|70794|6|Mentioned|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Youanmi Terrane, Yilgarn Craton. Also 2_5m_interpgeop15_lut.csv.|||Includes Big Bell Suite.|||
74824|Austin Downs Supersuite|70796|6|Mentioned|2_5m_interpgeop15_lut.csv|Neoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop.lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 155501.1.pdf, 155502.1.pdf, 155503.1.pdf, 155504.1.pdf, 155511.1.pdf,155505.1.pdf,155507.1.pdf, 185922.1.pdf, 185923.1.pdf, Austin100_2442_stratig.pdf, Badja100_2240_stratig.pdf, Cue100_2443_stratig.pdf, Madoonga100_2444_stratig.pdf, MountMagnet100_2441_stratig.pdf, Nowthanna100_2643_stratig.pdf, Reedy100_2543_stratig.pdf, Tieraco100_2545_stratig.pdf, Wynyangoo100_2542_stratig.pdf.|||Includes the Big Bell Suite, Yalgowra Suite.|||
74824|Austin Downs Supersuite|70830|5|Briefly described|p9|||Murchison Domain.|||Includes the Big Bell and Yalgowra suites.|||
74824|Austin Downs Supersuite|71159|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|||Big Bell Suite.||Metagranite.|
74824|Austin Downs Supersuite|71168|5|Briefly described|p7|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c. 2740-2690 Ma||Includes the Big Bell Suite.||Granitic rocks.|
74824|Austin Downs Supersuite|71269|5|Briefly described|GEOL_LUT_CSV files + geochron files|||Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv.|||Includes Big Bell Suite, Yalgowra Suite.|||
74824|Austin Downs Supersuite|71270|5|Briefly described|GEOL_LUT_CSV files|||Geological province: Yilgarn Craton, West Australian Craton. See 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|||Includes Big Bell Suite.|||
74824|Austin Downs Supersuite|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|||Yalgowra, Big Bell Suites.|||
74824|Austin Downs Supersuite|71272|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|||Big Bell Suite.|||
74824|Austin Downs Supersuite|71809|5|Briefly described|map legend|Archean|Archean|Yilgarn Craton, Youanmi Terrane|||Includes Big Bell Suite.|||
74824|Austin Downs Supersuite|72034|6|Mentioned|500k_interpgeop16_lut|Neoarchean|Neoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Big Bell Suite.|||
74824|Austin Downs Supersuite|72389|5|Briefly described|Map Legend|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Gabanintha 1:100k map sheet 2644.|2735-2686 Ma||Includes the Big Bell Suite.|||28-AUG-20
23346|Australind Formation|40367|2|Defined|p73|Middle Pleistocene|Middle Pleistocene|Unconformably overlies weathered sediments of Warnbro Group; disconformably overlain by Tamala Limestone. Thickness: 3m. Four sediment types including calcareous muds, calcareous sands and lithoclast gravel.||||||07-AUG-07
23346|Australind Formation|40400|6|Mentioned|p109|||Of Semeniuk (1983).||||||06-AUG-07
23346|Australind Formation|40401|6|Mentioned|p122|||||||||
39033|BB1|26357|6|Mentioned|not recorded|Grandispora spiculifera|Givetian|||||||19-FEB-08
39034|BB2|26357|6|Mentioned|not recorded|||||||||
39036|BB3|26357|6|Mentioned|not recorded|||||||||
39038|BB4|26357|6|Mentioned|not recorded|||||||||
39040|BB5|26357|6|Mentioned|not recorded|||||||||
39041|BB6|26357|6|Mentioned|not recorded|||||||||
39042|BB7|26357|6|Mentioned|not recorded|||||||||
39043|BB8a|14142|5|Briefly described|p24-27, Fig 23, Plate 2|Tithonian|Callovian|Described only as BB8 in this ref. The base of the supersequence (seismic horizon Jcal)  is defined as the base of the W. digitata dinocyst zone (DZ) (163 Ma).Overlying sediments are of R. aemula DZ . Age of top of the supersequence is: Top of Lower P. iehiense dinocyst zone. Minimum age of base of of BB8a could be ~at the boundary between W. spectabilis 6ci and the underlying W. spectabilis 6cii.||||Equivalent to lower Vulcan Formation, Montara Formation.|Lowstand fans and prograding deltaic sand and siltstone, transgressive shoreline sands, prograding distal highstand shales.|09-APR-19
39043|BB8a|26357|6|Mentioned|not recorded|||||||||
39044|BB8b|14142|5|Briefly described|p24-27, Fig 23, Plate 2|Tithonian|Callovian|Described only as BB8 in this ref. The base of the supersequence (seismic horizon Jcal)  is defined as the base of the W. digitata dinocyst zone (DZ) (163 Ma).Overlying sediments are of R. aemula DZ . Age of top of the supersequence is: Top of Lower P. iehiense dinocyst zone.||||Equivalent to lower Vulcan Formation, Montara Formation.|Lowstand fans and prograding deltaic sand and siltstone, transgressive shoreline sands, prograding distal highstand shales.|09-APR-19
39044|BB8b|26357|6|Mentioned|not recorded|||||||||
39045|BB8c|14142|5|Briefly described|p24-27, Fig 23, Plate 2|Tithonian|Callovian|Described only as BB8 in this ref. The base of the supersequence (seismic horizon Jcal)  is defined as the base of the W. digitata dinocyst zone (DZ) (163 Ma).Overlying sediments are of R. aemula DZ . Age of top of the supersequence is: Top of Lower P. iehiense dinocyst zone.||||Equivalent to lower Vulcan Formation, Montara Formation.|Lowstand fans and prograding deltaic sand and siltstone, transgressive shoreline sands, prograding distal highstand shales.|09-APR-19
39045|BB8c|26357|6|Mentioned|not recorded|||||||||
39046|BB9|26357|6|Mentioned|not recorded|||||||||
24679|Backdoor Formation|22694|5|Briefly described|p8|||Collier Subgroup, Bangemall Basin||||||
24679|Backdoor Formation|22716|6|Mentioned|p237|Ectasian|Ectasian|||||||
24679|Backdoor Formation|22897|6|Mentioned|102|||Geol province Bangemall Basin||||||
24679|Backdoor Formation|22905|5|Briefly described|p52 Fig. 2, p53 Table 1, p54|Mesoproterozoic|Mesoproterozoic|Of the Collier Group. Previously known as Fords Creek Shale (Mucalana Subgroup). Overlying unit: Calyie Formation; underlying unit: Edmund Group.  Max. thickness: 1500m.||||||24-JAN-06
24679|Backdoor Formation|22940|4|Described|p20, p21|Mesoproterozoic|Mesoproterozoic|Of the Collier Subgroup. Overlying unit: Calyie Sandstone, underlying unit: Wonyulgunna Sandstone.||||||14-NOV-11
24679|Backdoor Formation|23156|5|Briefly described|p9|Mesoproterozoic|Mesoproterozoic|Unit gently folded and passes unconformably eastwards beneath the Savory Group.  In the northwestern corner of BULLEN the unit is overlain by Calyie Formation (conformity).  On BULLEN underlying unit - Wonyulgunna Sandstone (conformity).||||||
24679|Backdoor Formation|23723|6|Mentioned|p11|||Geological Province: Bangemall Basin.||||||
24679|Backdoor Formation|23747|5|Briefly described|p16|||Of Bangemall Group. Geological Province: Bangemall Basin.||||||
24679|Backdoor Formation|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Bangemall Group. Geological Province: Bangemall Basin.||||||
24679|Backdoor Formation|23749|4|Described|p15|Proterozoic|Proterozoic|Of Bangemall Group. Geological Province: Bangemall Basin.||||||
24679|Backdoor Formation|23750|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Bangemall Group. Geological Province: Bangemall Basin.||||||
24679|Backdoor Formation|24017|6|Mentioned|p23|||||||||
24679|Backdoor Formation|24115|4|Described|p4 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the Collier Group. Maximum Thickness: 1500m. Unconformably overlies the Coodardoo Formation. Overlain by the Calyie Formation. Geological Province: Collier Basin.||||||
24679|Backdoor Formation|24183|2|Defined|p4 Fig.3, p20|Stenian|Ectasian|Lowermost unit of the Collier Group (Martin et al. 1999a). Max. Thickness: 1740m. Disconformably overlies the Coodardoo Formation. Overlain by the Calyie Formation. Age: c. 1211-1070 Ma.||||||
24679|Backdoor Formation|24544|4|Described|p44 Fig.32|Mesoproterozoic|Mesoproterozoic|Of Collier Group. Superseded Fords Creek Shale. Overlies Coodardoo Formation. Overlain by Calyie Formation.||||||
24679|Backdoor Formation|29916|4|Described|p119|||||||||
24679|Backdoor Formation|33849|4|Described|p126|||||||||
24679|Backdoor Formation|36551|6|Mentioned|p101|||||||||
24679|Backdoor Formation|37018|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24679|Backdoor Formation|37024|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24679|Backdoor Formation|37026|4|Described|p4|||||||||
24679|Backdoor Formation|37213|5|Briefly described|p22|||||||||
24679|Backdoor Formation|37460|4|Described|p164|||||||||
24679|Backdoor Formation|37707|6|Mentioned|Table I|||||||||
24679|Backdoor Formation|38298|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24679|Backdoor Formation|38299|4|Described|p12|||||||||
24679|Backdoor Formation|38515|6|Mentioned|Table 1|||||||||
24679|Backdoor Formation|39168|6|Mentioned|p71|||||||||
24679|Backdoor Formation|39171|6|Mentioned|p82|||||||||
24679|Backdoor Formation|39697|6|Mentioned|p130|||||||||
24679|Backdoor Formation|40088|6|Mentioned|p228|||||||||
24679|Backdoor Formation|40089|2|Defined|p45|Mesoproterozoic|Mesoproterozoic|||||||
24679|Backdoor Formation|40899|6|Mentioned|Fig.1|||||||||
24679|Backdoor Formation|40989|4|Described|p33|||Mention Fig.1||||||
24679|Backdoor Formation|41360|6|Mentioned|Table 1|||||||||
24679|Backdoor Formation|42013|5|Briefly described|Map Legend|Proterozoic||||||||
24679|Backdoor Formation|43209|5|Briefly described|map legend||Mesoproterozoic|Of Collier Subgroup.||||||
24679|Backdoor Formation|43238|5|Briefly described|p7|||||||||
24679|Backdoor Formation|43492|6|Mentioned|12|||||||||
24679|Backdoor Formation|43830|5|Briefly described|Map Legend||Mesoproterozoic|||||||
24679|Backdoor Formation|44142|4|Described|p311-312, p315, p318-319, p321-323|||~3700m thick open-marine shelf and distal turbidite deposits. Chuck (1984) equated this Formation with Dooley Subgroup; Muhling and Brakel (1985) equated it with all units between Irregully Formation and Mount Vernon Sandstone. Correlate of Fords Creek Shale. Lateral equivalent of Manganese Subgroup units.|<1098 +/- 42 Ma.|Collier Subgroup||Overlies Coobarra Formation and Wonyulgunna Sandstone conformably. Is overlain conformably by Calyie Sandstone and Stag Arrow Formation.|Shale, siltstone; lesser chert, claystone, dolomite, sandstone.|13-MAR-18
24679|Backdoor Formation|50010|5|Briefly described|p54|Mesoproterozoic|Mesoproterozoic|Sandstone, siltstone and dolostone. Thickness: 1.7km. Deposited below storm wave-base. Overlain by Calyie Formation.||||||
24679|Backdoor Formation|50225|4|Described|p387 Fig. 2, p396|||Of Collier Gp (Bangemall Supergroup).  Supersedes Fords Creek Shale (Bangemall Gp). Predominantly laminated siltstone + minor thin beds of fine-grained sandstone. Gradational contact with Calyie Fm above.  Max. thickness: 1500m.||||||07-FEB-11
24679|Backdoor Formation|50226|6|Mentioned|p429|||Of the Collier Group.||||||
24679|Backdoor Formation|50292|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Collier Basin.  Of the Collier Group (Bangemall Supergroup).||||||
24679|Backdoor Formation|50380|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Collier Group (Bangemall Supergroup). Geological Province: Collier Basin.||||||07-NOV-08
24679|Backdoor Formation|60301|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Collier Group (Bangemall Supergroup). Geological Province: Collier Basin. Siltstone, mudstone, sandstone, minor chert and dolostone.||||||20-AUG-04
24679|Backdoor Formation|60535|5|Briefly described|p556, 557|Mesoproterozoic|Mesoproterozoic|Of the Collier Group (Bangemall Supergroup). Maximum thickness: 1700 m. Laminated mudstone, minor sandstone interbeds.||||||
24679|Backdoor Formation|62453|6|Mentioned|p53|||||||||
24679|Backdoor Formation|63471|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Collier Group (Bangemall Supergroup). Geological Province: Collier Basin. Siltstone, mudstone, thin- to thick-bedded sandstone; minor chert and dolostone.||||||14-NOV-11
24679|Backdoor Formation|63866|5|Briefly described|p162-p163|Ectasian|Calymmian|Intruded by a suite of dolerite sills which constrain the minimum age of the Collier Group.|1352 +/- 89 Ma (Cawood and Nemchin, 2002)|Collier Group||||
24679|Backdoor Formation|63869|5|Briefly described|p39-41, p42, Plate 1|Mesoproterozoic|Mesoproterozoic|150 m thick. Maximum age from detrital zircons (Cawood and Nemchin, 2002); minimum age from dolerite sills (Wingate, 2002).|c.1400-c.1070 Ma.|Unit in Collier Group.||Overlies Wonyulgunna Sandstone (where present). Disconformably overlies Coodardoo Formation. Is overlain gradationally by Calyie Formation.|Planar-laminated green, maroon and cream-coloured siltstone and mudstone, interbedded with subordinate fine- to very coarse-grained lithic sandstone, dolostone and minor thin chert beds; intruded by dolerite sills.|
24679|Backdoor Formation|64580|6|Mentioned|map legend||Mesoproterozoic|Of Collier Group. Part of depositional package 5 (Backdoor and Calyie Formations).||||||15-DEC-08
24679|Backdoor Formation|64728|5|Briefly described|p95 Fig.2, pp105-107.|Mesoproterozoic|Mesoproterozoic|Shallowing-upwards deep marine siliciclastic facies.||Unit in Collier Group.||Overlies Coodardoo Formation. Is overlain by Calyie Formation.|Thick-bedded, fine- to coarse-grained quartz sandstone.|
24679|Backdoor Formation|64772|5|Briefly described|p13, p25 Fig. 12, Plate 1|Mesoproterozoic|Mesoproterozoic|Of the Collier Group. Geological province: Collier Basin. Siltstone, mudstone, and thin- thick-bedded sandstone; minor chert and dolostone.||||||25-NOV-13
24679|Backdoor Formation|65830|3|Fully described|p7-p11, p16-19; Plates 1,2|Stenian|Calymmian|Age determined from detrital zircons. ~1500m thick. Locally intruded by discordant dolerite sills. Records a progradation from distal shelf to proximal shelf and distal delta-front depositional environments. Contains abundant megafossils ('strings of beads') within its lower part.|c.1620 Ma (Martin et al., in press).|Of the Collier Group||Gradationally overlain by the Calyie Formation. Unconformably underlain by the Coodardoo Formation.|Consists of planar-laminated green, maroon, and cream-coloured siltstone and mudstone, interbedded with subordinate very coarse to fine-grained lithic sandstone, oolitic dolostone, and minor thin chert beds.|
24679|Backdoor Formation|65896|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Unit in Collier Group, Bangemall Supergroup. Grey to brown shale, with cream to grey laminated chert.||||||
24679|Backdoor Formation|66104|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Unit in lower Collier Group. Siltstone, mudstone, and thin- to thick-bedded sandstone; minor chert and dolostone. Includes two mapped but unnamed units; one of chert and siltstone, the other of thin- to thick-bedded sandstone and siltstone.||||||
24679|Backdoor Formation|66107|5|Briefly described|p1-5, p7, p9-12, p14   |Mesoproterozoic|Mesoproterozoic|Contains 'string of beads' macrofossils, formally named in this article as Horodyskia williamsii and systematically described.||Of the Collier Group||Correlative of Stag Arrow Formation.||
24679|Backdoor Formation|66112|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Unit in Collier Group. Siltstone, mudstone, and thin- to thick-bedded sandstone; minor chert and dolostone. Includes a mapped but unnamed unit of thin- to thick-bedded sandstone and siltstone.||||||
24679|Backdoor Formation|66241|5|Briefly described|pp1-4, p9. |Mesoproterozoic|Mesoproterozoic|||Basal unit in Collier Group.||Overlies Coodardoo Formation. Is overlain by Calyie Formation.|Deep marine mudstone; subordinate thin- to thick-bedded sandstone; minor chert and dolostone.|
24679|Backdoor Formation|66948|6|Mentioned|p22|||Below storm wavebase. Contains H. williamsii.|||||Dark pyritic shale.|
24679|Backdoor Formation|67136|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin.||Unit in Collier Group.||Is overlain by Calyie Formation.|Siltstone, mudstone, sandstone; minor dolostone, chert and conglomerate.|
24679|Backdoor Formation|67245|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin.||Unit in Collier Group.|||Thin- to thick-bedded sandstone and minor siltstone.|
24679|Backdoor Formation|67374|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin.||Unit in Collier Group.|Includes Jeeaila Sandstone Member.||Siltstone, mudstone, and thin- to thick-bedded sandstone; minor chert and dolostone.|
24679|Backdoor Formation|68285|5|Briefly described|Map Legend|Stenian|Calymmian|Collier Basin.||Of the Collier Group.|Informally subdivided in part into two unnamed units.|Underlain by the Ullawarra Formation. Overlain by the Calyie Formation.|Siltstone, mudstone, and thin- to thick-bedded sandstone; minor chert and dolostone; thin- to thick-bedded sandstone and minor siltstone; thin- to thick-bedded dololutite, dolomitic siltstone, dolarenite, and siltstone.|
24679|Backdoor Formation|68286|5|Briefly described|Map Legend|Stenian|Calymmian|Collier Basin.||Of the Collier Group|Includes Jeeaila Sandstone Member and 3 other unnamed members.|Underlain by the Ullawarra Formation. Overlain by the Calyie Formation.|Siltstone, mudstone, and thin- to thick-bedded sandstone; minor chert and dolostone.|
24679|Backdoor Formation|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv|Mesoproterozoic|Mesoproterozoic|Described together with Calyie Formation as: siltstone, mudstone, sandstone; minor dolostone, chert, and conglomerate.||Collier Group||||22-OCT-15
24679|Backdoor Formation|69003|4|Described|p34, p53|Mesoproterozoic|Mesoproterozoic|Collier Basin, Capricorn Orogen. Forms extensive peperite, indicating recently deposited wet sediment at time of intrusion (viz. c.1070 Ma).||Collier Group.||Overlies Coodardoo Formation (Edmund Group). Is overlain by Calyie Formation.|Deep-marine siliciclastic sediments.|
24679|Backdoor Formation|69010|5|Briefly described|Map Legend|Stenian|Calymmian|Collier Basin. Four facies are mapped separately: thin- to thick-bedded dololutite, dolomitic siltstone, dolarenite and siltstone; chert and siltstone; thin- to thick-bedded sandstone and siltstone; and thin- to thick-bedded sandstone and minor siltstone.|1460-1070 Ma|Of the Collier Group.|||Comprises siltstone, mudstone, and thin- to thick-bedded sandstone; minor chert and dolostone.|24-APR-14
24679|Backdoor Formation|69027|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Collier Basin. Includes 2 unnamed subunits mapped separately.||Of the Collier Group.||Underlain by the Coodardoo Formation. Overlain by the Calyie Formation.|Siltstone, mudstone, and thin- to thick-bedded sandstone, minor chert and dolostone; thin- to thick-bedded sandstone and siltstone; dololutite, dolomitic siltstone, dolarenite and siltstone.|05-MAY-14
24679|Backdoor Formation|69028|5|Briefly described|Map Legend|Stenian|Stenian|Collier Basin. Mapped with Calyie Formation as a single unit.||Of the Collier Group.|||Siltstone, mudstone and sandstone; minor dolostone, chert and conglomerate.|06-MAY-14
24679|Backdoor Formation|69091|5|Briefly described|p202|||Collier Basin. Thickness: ~1500 m|||||Laminated siltstones, with some fine-grained sandstone and thin-bedded mudstone.|
24679|Backdoor Formation|69166|4|Described|geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Age derived from quartz sandstone samples (156541.1.pdf, 148977.1.pdf)|1619 +/- 17 Ma, 1790 +/-4 Ma (SHRIMP)|Collier Group||Disconformably overlies Coodardoo Formation, Overlain by Calyie Formation|Chert and mudstone, thin-thickly bedded dololutite, dolomitic siltstone, dolarenite,  thin-thickly bedded sandstone and siltstone.|
24679|Backdoor Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|||Part of Collier Group Depositional package 5.||Unit of Collier Group.||||
24679|Backdoor Formation|69553|5|Briefly described|p62|Mesoproterozoic|Mesoproterozoic|Contains Horodyskia fossils, and possible correlative to the Cassiterite Creek Quartzite of the Balfour Subgroup, but much younger than the Cassiterite Creek Quartzite.|1200-1070 Ma|Unit of Bangemall Supergroup.||||
24679|Backdoor Formation|69596|5|Briefly described|p12 Fig.7, p13, p30|||Collier Basin. Has peperitic textures locally at Kulkatharra Dolerite sills, implying intrusion into unconsolidated sediments as well as giving a depositional age (c.1070 Ma).||Basal Collier Group.||||
24679|Backdoor Formation|70132|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Collier Basin. Four facies associations are mapped separately.||Collier Group.||Is overlain by Calyie Formation.|Siltstone, mudstone, thin- to thick-bedded sandstone, minor chert and dolostone. Chert and siltstone; sandstone and minor siltstone; dolostone, dolomitic siltstone, siltstone and sandstone; silicified chert breccia, conglomerate, sandstone (section).|
24679|Backdoor Formation|70136|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Collier Basin. Three facies associations are mapped separately.||Collier Group.|||Siltstone, mudstone and thin- to thick-bedded sandstone, minor chert and dolostone. Chert and siltstone; thin- to thick-bedded sandstone and siltstone; thin- to thick-bedded dololutite, dolomitic siltstone, dolarenite and siltstone (section only).|
24679|Backdoor Formation|70767|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin. Three un-named sub-units are mapped separately: thin- to thick-bedded sandstone and siltstone; thin- to thick-bedded sandstone and minor siltstone; thin- to thick-bedded dololutite, dolarenite, dolorudite, dolomitic siltstone, siltstone and sandstone.||Collier Group.||Overlies Ullawarra Formation. Is overlain by Calyie Formation. Is intruded by Kulkatharra Dolerite.|Siltstone, mudstone, and thin- to thick-bedded sandstone; minor chert and dolostone.|
24679|Backdoor Formation|70768|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin.||Collier Group.||Overlies Ullawarra Formation. Is overlain by Calyie Formation. Is intruded by Kulkatharra Dolerite.|Siltstone, mudstone, and thin- to thick-bedded sandstone; minor chert and dolostone. One un-named sub-unit is mapped separately: thin- to thick-bedded dololutite, dolarenite, dolorudite, dolomitic siltstone, siltstone and sandstone.|
24679|Backdoor Formation|70795|4|Described|100k_geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Also 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 148976.1.pdf, 156541.1.pdf, West Australian Craton, Collier Basin|1171-1070 Ma|Collier Group||Disconformably overlies Coodardoo Formation, Overlain by Calyie Formation, overlies Edmund Group|Siltstone, mudstone, thin to thick bedded quartz sandstone, chert, chert breccia, conglomerate, dolostone, dololutite, dolarenite, dolorudite and dolomitic siltstone.|
24679|Backdoor Formation|70814|4|Described|p5, p15-p16, p20, p22, p25-p28, p37, p57|||Collier Basin. This unit is seperated informally into a lower (deep marine shelf sedimentation) and an upper component (delta progradation). Outcrop characteristics discussed. This unit ranges in thickness from 1400 to 1750m in the Wanna Syncline. This unit was deposited in distal shelf to proximal shelf and distal delta-front environments.|c. 1397 Ma|Collier Group||Unconformably overlies the Coodardoo Formation and the Ullawarra Formation. Unconformably overlies the Bryah Group. Conformably overlain by the Calyie Formation.|Siltstone, mudstone, thin to thickly-bedded sandstone and minor chert and dolomite.|
24679|Backdoor Formation|70936|5|Briefly described|p61,74|Mesoproterozoic|Mesoproterozoic|Geological province: Pilbara Craton. Lower 1500m section contains enigmatic strings of beads macrofossils (Horodyskia williamsii; Grey et al., 2010) which have been identified at 49 localities over at least 500 km of strike length (Grey and Williams, 1990; Grey et al., 2002, 2010; Martin, 2004), representing an important biomarker not seen anywhere else in the Bangemall Supergroup stratigraphy.||Unit of Bangemall Supergroup.||||
24679|Backdoor Formation|71003|6|Mentioned|p61, p74|Mesoproterozoic|Mesoproterozoic|Pilbara Craton.||Collier Group||||
24679|Backdoor Formation|71158|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin. Two facies associations are mapped separately: chert and siltstone; and thin- to thick-bedded sandstone and minor siltstone.||Collier Group.|||Siltstone, mudstone and thin- to thick-bedded sandstone; minor chert and dolostone.|
24679|Backdoor Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone, crystalline dolostone/dolomite, shale, sedimentary breccia|
24679|Backdoor Formation|71269|5|Briefly described|1m_geologyp12_lut.csv|||Geological province: Capricorn Orogen; West Australian Craton. ||Unit of Collier Group.|||Shale, siltstone, minor fine-grained sandstone, chert, mudstone, dolostone.|
24679|Backdoor Formation|72259|6|Mentioned|p3|||||Collier Group||||
24679|Backdoor Formation|72705|5|Briefly described|p3|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||Collier Group.||Overlies Coodardoo Formation. Is overlain by Calyie Formation.||
24679|Backdoor Formation|73442|5|Briefly described|p20, p23|||Also referred to as Depositional Package 5.||||Intruded by Kulkatharra Dolerite|Includes dolomite, siltstone and fine-grained sandstone.|
23351|Baghdad Member|41831|5|Briefly described|p558|||See also Fig.3||||||
75570|Baines beds|65074|4|Described|p349, p351 fig 4-37, p352, p355 Tb. 4-11|Mesoproterozoic|Mesoproterozoic|Of NW Birrindudu Basin. Tightly folded; more deformed than Birrindudu Group. ~1000m thick. Reference area details given.||||Probably equivalent to Talbot Well Formation and Gardiner Sandstone.|Arenite and shale, conglomerate, siltstone, glauconitic and dolomitic sandstone. Mudstone at top.|
75570|Baines beds|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Shallow marine medium to thinly bedded, rippled and cross bedded sublithic sandstone and quartz sandstone with a sparse clayey matrix; minor lithic sandstone, greywacke, conglomerate and siltstone, with mudstone at the top|
74836|Bald Rock Supersuite|64891|5|Briefly described|p34 Fig.1, p37 Fig. 2, p42, p52-53 Tb.1|Archean|Archean|Contains Wogala and Walganna Suites. Age: 2637-2592Ma. Geological province: Murchison Domain. Post-tectonic monzogranite, syenogranite, and alkali granite.||||||07-FEB-11
74836|Bald Rock Supersuite|65546|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Yilgarn Craton. 2637-2602 Ma. Includes Walganna Suite. ||||||
74836|Bald Rock Supersuite|65548|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Yilgarn Craton. Includes Walganna Suite,  Wogala Suite: Granites and undivided metamorphics. Age shown for Walganna Suite: 2637-2602 Ma.||||||
74836|Bald Rock Supersuite|65550|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Includes Walganna Suite. Age of 2637-2602 Ma given. ||||||
74836|Bald Rock Supersuite|66195|5|Briefly described|p599 Fig.2|Neoarchean||Granitic rocks including the Wogala and Walganna Suites.||||||13-MAR-12
74836|Bald Rock Supersuite|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|||Includes Walganna Suite.|||
74836|Bald Rock Supersuite|67129|6|Mentioned|p18 Fig.19, p19 Fig.20|Archean|Archean|Murchison Domain, Youanmi Terrane.|2640-2600 Ma||Walganna Suite, Wogala Suite; Taincrow, Garden Rock, Telegootherra Monzogranites.|||06-SEP-17
74836|Bald Rock Supersuite|68108|5|Briefly described|p628, p649|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane.|ca. 2637-2592 Ma||||Post-tectonic monzogranites.|
74836|Bald Rock Supersuite|68519|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|2640-2610 Ma||Includes Walganna Suite and Wogala Suite.|||
74836|Bald Rock Supersuite|68561|5|Briefly described|GEOL_LUT_CSV folder + GEOCHRON files|||Murchison Domain, Youanmi Terrane. Age: 2640-2605 Ma. See geochron file 185929.1.pdf.|||Includes Wogala Suite, Walganna Suite|||
74836|Bald Rock Supersuite|68698|5|Briefly described|p1, p3-5, p8, p10-11, p14-15, p18-21|Neoarchean|Neoarchean|Post-tectonic, undeformed granites. Geochemistry is discussed in detail. Lu-Hf isotope data and source regions discussed. REE plots.|c.2630-2600 Ma.||Walganna and Wogala Suites.|||
74836|Bald Rock Supersuite|69014|6|Mentioned|Map Legend|Neoarchean|Neoarchean|Murchison Domain.|||Includes Walganna Suite.|||
74836|Bald Rock Supersuite|69583|4|Described|p44, p49, p51-53, p56, p101, p105, p109|Neoarchean|Neoarchean|See also p118-119, p126, p130; Plates 2, 3. Northern Youanmi Terrane. Post-tectonic granites. c.2-3km thick. Seismic interpretation.|<2638-2592 Ma.||Walganna, Wogala Suites.||Undeformed granites and monzogranites.|
74836|Bald Rock Supersuite|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean||||Walganna Suite, Wogala Suite|||
74836|Bald Rock Supersuite|69586|5|Briefly described|p7, p22|Neoarchean|Neoarchean||<2638-2592 Ma.||||Post-tectonic granites.|
74836|Bald Rock Supersuite|69626|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton|||Walganna Suite|||
74836|Bald Rock Supersuite|69627|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton|||Walganna Suite|||
74836|Bald Rock Supersuite|69628|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton|||Walganna Suite|||
74836|Bald Rock Supersuite|69744|6|Mentioned|p254, 262|||Post-tectonic.|2640-2600 Ma.|||||
74836|Bald Rock Supersuite|70020|5|Briefly described|p118|Neoarchean|Neoarchean|Geological province: Yilgarn Craton.|||Includes Wogala and Walganna suites.|Underlain by Jungar Suite.||
74836|Bald Rock Supersuite|70030|5|Briefly described|p191-192|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton.|2640-2600 Ma||Includes Wogala and Walganna suites, and Taincrow Monzogranite and Telegootherra Monzogranite.||Monzogranite.|17-JUL-19
74836|Bald Rock Supersuite|70139|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton.|||Walganna Suite.|||
74836|Bald Rock Supersuite|70140|5|Briefly described|Map legend.|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|2640-2600 Ma.||Walganna Suite.|||
74836|Bald Rock Supersuite|70156|4|Described|500k_interpgeop14_lut.csv|||Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma).|||Includes Walganna Suite.|||
74836|Bald Rock Supersuite|70226|5|Briefly described|map legends|Archean|Archean|Yilgarn Craton.|||Walganna Suite|||
74836|Bald Rock Supersuite|70332|6|Mentioned|p79|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|2640-2600 Ma.||||Post-tectonic granites.|
74836|Bald Rock Supersuite|70419|5|Briefly described|p3, p10, p13-14, p17, p21, p26 Fig.10|Neoarchean|Neoarchean||2640-2600 Ma.||Wogala Suite.|Intrudes the Windimurra Igneous Complex.|Post-tectonic granites.|
74836|Bald Rock Supersuite|70420|5|Briefly described|p5,p9-11,p16-19,p21,p24,p26-27,p31-32|Archean|Archean|3D modelling described; density and magnetic susceptibility values given.|||||Post-tectonic granite.|
74836|Bald Rock Supersuite|70769|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton.|2647-2600 Ma.||Walganna Suite.|||03-MAR-17
74836|Bald Rock Supersuite|70770|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton.|2647-2600 Ma.||Walganna Suite.|||
74836|Bald Rock Supersuite|70794|6|Mentioned|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean||||Includes Walganna Suite.|||
74836|Bald Rock Supersuite|70796|6|Mentioned|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton. See also 100k_geologyl_lut.csv, 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 155513.1.pdf, 178197.1.pdf, 185929.1.pd, 185997.1.pdf, 198212.1.pdf, 198220.1.pdf, 207630.1.pdf, Austin100_2442_stratig.pdf, Badja100_2240_stratig.pdf, Bungar100_2539_stratig.pdf, Coolamaninu100_2540_stratig.pdf, Cue100_2443_stratig.pdf, Koonmarra100_2445_stratig.pdf, Madoonga100_2444_stratig.pdf, Nowthanna100_2643_stratig.pdf, Reedy100_2543_stratig.pdf, Tieraco100_2545_stratig.pdf, Windimurra100_2641_stratig.pdf, Wynyangoo100_2542_stratig.pdf, Yalgoo100_2241_stratig.pdf, Youanmi100_2640_stratig.pdf.|ca 2647 to 2600 Ma (inferred)||Inclues the Wogala Suite and the Walganna Suite.|Crosscuts the Tuckanarra Suite.||
74836|Bald Rock Supersuite|70830|5|Briefly described|p8-p10, p29, p33, p40, p51, p58|Neoarchean|Neoarchean|Murchison Domain. |c.2640-2600 Ma||Includes the Walganna Suite and Wogala Suite.||Monzogranites.|
74836|Bald Rock Supersuite|71159|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton.|||Walganna Suite.|||
74836|Bald Rock Supersuite|71168|5|Briefly described|p7|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c. 2630-2600 Ma||Includes the Walganna and Wogala Suites.||Granitic rocks.|
74836|Bald Rock Supersuite|71269|5|Briefly described|GEOL_LUT_CSV files + geochron files|||Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv.|||Includes Walganna Suite, Wogala Suite.|Crosscuts Cundimurra Monzogranite/Tuckamarra Suite.||
74836|Bald Rock Supersuite|71270|5|Briefly described|GEOL_LUT_CSV files|||Geological province: Yilgarn Craton, West Australian Craton. See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv.|||Includes Walganna Suite.|||
74836|Bald Rock Supersuite|71271|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton.|2650-2600 Ma.||Walganna Suite.|||
74836|Bald Rock Supersuite|71272|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton.|||Walganna Suite.|||
74836|Bald Rock Supersuite|71311|5|Briefly described|p794, p798|||Northern Youanmi Terrane, Yilgarn Craton. Appears as Bald rock supersuite on p794.|<2638-2592 Ma.||Telegootherra Monzogranite.|||19-DEC-18
74836|Bald Rock Supersuite|71809|5|Briefly described|map legend|Archean|Archean|Yilgarn Craton|||Includes Walganna Suite.|||
74836|Bald Rock Supersuite|72034|6|Mentioned|500k_interpgeop16_lut|Neoarchean|Neoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Wogala Suite.|||
74836|Bald Rock Supersuite|72389|5|Briefly described|Map Legend|Archean|Archean|Yilgarn Craton. Gabanintha 1:100k map sheet 2644.|2650-2600 Ma||Includes the Walganna Suite|||28-AUG-20
74836|Bald Rock Supersuite|73023|5|Briefly described|p2-3|Neoarchaean|Neoarchaean|One sample is dated at 2626 +/- 6 Ma.|2640-2600 Ma.||Seeligson Monzogranite.|Intrudes Goonetarra Granodiorite and Kynea Tonalite.|Post-tectonic granitoids. A-type to low-Ca granitoids.|
74836|Bald Rock Supersuite|73410|5|Briefly described|p2, p3 Fig.2|||Youanmi Terrane.  Comprises discordant tabular bodies with flat-lying floors; extend ~3-5 km below current exposure level.|2640-2600 Ma.||||Late-orogenic granites. Invariably undeformed.|
74836|Bald Rock Supersuite|73596|6|Mentioned|p1168|Neoarchean|Neoarchean|Yilgarn Craton.|2640-2600 Ma.|||||
24169|Baleine Formation|13255|6|Mentioned|p369|Late Jurassic|Late Jurassic|Roebuck Basin.||||Unconformably overlies Depuch Formation. Is overlain by Egret Formation.||
24169|Baleine Formation|41732|6|Mentioned|Fig.3|||||||||
24169|Baleine Formation|44143|4|Described|p.432 Table 4-19; p.449|Jurassic|Jurassic|>600m thick, claystone and interbedded sandstone and siltstone; marine. Type section 904-1272m in Lacepede 1A (17deg 5' 18" S, 121deg 26' 41" E); palynology indicates a late Tithonian to early Neocomian age.||||||22-NOV-17
24169|Baleine Formation|45153|2|Defined|App.7-127|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous.||||||
24169|Baleine Formation|69297|6|Mentioned|p337, p339, p352|Tithonian|Tithonian|Canning and Roebuck Basins. Contains potential sealing shales. ||||Unconformably overlies the Depuch Formation. Overlain by the Egret Formation or unconformably overlain by the Mermaid Formation.||
24169|Baleine Formation|70065|5|Briefly described|Rowley: Fig.2; p2. Regional: Fig.4; p4|Berriasian|Tithonian|Roebuck Basin and offshore Canning Basin. Claystones form a regional seal.||||Unconformably overlies Depuch Formation. Coverlain by Egret Formation. Is conformably to unconformably overlain by Mermaid Formation.|Condensed marine mudstones.|01-MAY-19
25772|Balfour Formation|41669|2|Defined|Table 5|Precambrian?||||||||
25772|Balfour Formation|41768|4|Described|p44|||||||||
25772|Balfour Formation|43055|3|Fully described|Table 4, Table 5|||of Manganese Group||||||
25772|Balfour Formation|43056|5|Briefly described|Map Legend|||of Manganese Group||||||
25772|Balfour Formation|44142|4|Described|p315 Tb. 4-4, p322-324|||~1500m thick suspension deposits in marine lagoons and sub-basins; distal turbidites in basins. This name includes and supersedes "Balfour Shale" and "Noreena Shale" (de la Hunty, 1963). Manganese-enriched shale resembles that of the Ilgarari Formation. Many dolerite sills.||Manganese Subgroup||Overlies Stag Arrow Formation disconformably, as well as Jigalong Formation and Enacheddong Dolomite when present. Overlies Coondoon Formation disconformably. Correlates with Ilgarari Formation.|Shale; minor siltstone, calcareous siltstone, glauconitic fine grained sandstone. Has a distinctive basal Mn-enriched, grey-green shale.|07-JUL-20
25772|Balfour Formation|60535|5|Briefly described|p556 Fig.1|Mesoproterozoic|Mesoproterozoic|Of the Manganese Group (Bangemall Supergroup).||||||
25772|Balfour Formation|66107|5|Briefly described|p4 Fig.1 |Mesoproterozoic|Mesoproterozoic|||Of the Manganese Group||Overlies Jigalong Formation.||
25772|Balfour Formation|67183|5|Briefly described|p641,43, 45,47,49 53,55,61-2,68-69,71|Mesoproterozoic|Mesoproterozoic|Minor Mn mineralisation observed as stratiform deposits within a thick shale-siltstone sequence (e.g. Booginia Hill deposit). Present in the Oakover Basin||Manganese Subgroup||Conformably overlies the Stag Arrow Formation, suggested correlative of the Waltha Woora Formation.|Hosts Mn mineralisation/deposits. ~1500m thick sequence of shales, siltstone, dolomitic siltstone and minor fine-grained sandstone and dolomite.|
25772|Balfour Formation|71042|4|Described|p66 fig 2, p67|Mesoproterozoic|Mesoproterozoic|Oakover Basin. 1500m thick. Hosts the Nicholas Downs (or Booginia Hill) manganese deposit. See also p67-p69, p73, p82-p83.||Manganese Group||Conformably overlies the Stag Arrow Formation. Overlies the Enacheddong Dolomite. Intruded by the Davis Dolerite.|Shales, siltstone, dolomitic siltstone and minor fine-grained sandstone and dolomite.|24-MAY-19
25772|Balfour Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||sandstone, greensand, silstone, shale|
79384|Balgara Dolerite|72034|6|Mentioned|500k_interpgeop16_lut|||Mentioned as intruding sills.||||Intrudes Kungarra Formation, Cheela Springs Basalt, Shingle Creek Group, Turee Creek Group, as sills.||
79384|Balgara Dolerite|72712|4|Described|pp1, p19, p25, p35-37,p39,41,42,44-46.|Rhyacian|Rhyacian|New. Noted as a new unit in report (p35). SHRIMP U-Pb baddeleyite crystallisation age determined by Muller et al. (2005). It is proposed that this name Balgara be applied to all c. 2208 Ma sills, as well as any undated sills with similar geochemistry that intrude the Turee Creek or basal Shingle Creek Groups. Petrogenetically related to Cheela Springs Basalt. See also p48-49, p53, p55, p57, p9, p20, p29, p36 Fig.25, p37, p43.|2208+/-10 Ma SHRIMP U-Pb baddeleyite|||Intrudes Turee Creek Group, Shingle Creek Group. Said p19 to intrude between Calgra Member and Anthiby Formation, Turee Creek Group.|Shown as sills that include medium grained dolerite.|14-JAN-21
24684|Bali Monzogranite|41786|4|Described|p330|||||||||
24684|Bali Monzogranite|42382|5|Briefly described|p38|||||||||
24684|Bali Monzogranite|42626|6|Mentioned|Fig.14 P39|||||||||
24684|Bali Monzogranite|42697|5|Briefly described|map legend|||||||||
24684|Bali Monzogranite|42698|5|Briefly described|map legend|||||||||
24684|Bali Monzogranite|42740|5|Briefly described|map legend|Archean||||||||07-NOV-08
24684|Bali Monzogranite|42892|4|Described|p45|||||||||
24684|Bali Monzogranite|43074|6|Mentioned|p17|||||||||
24684|Bali Monzogranite|43102|6|Mentioned|p9|||||||||
24684|Bali Monzogranite|43125|4|Described|p9, and map insert|Archean|Archean|||||||03-MAR-10
24684|Bali Monzogranite|43232|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
24684|Bali Monzogranite|60076|5|Briefly described|p45 App. 1|Archean|Archean|[Agmbl] Coarse-grained, K-feldspar megacrysts.||||||07-NOV-08
24684|Bali Monzogranite|65204|6|Mentioned|p18 Tbl.3.|Neoarchean||3-7mm grains; porphyritic||||||
24684|Bali Monzogranite|65264|5|Briefly described|p46 Appdx. 1|Archean|Archean|Coarse-grained monzogranite with K-feldspar megacrysts; internally massive, intense contact-parallel foliation with down-dip mineral lineation.||||||07-FEB-11
24684|Bali Monzogranite|65834|6|Mentioned|p49-50|||Coolgardie Goldfield.||||||
24684|Bali Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Coarse-grained monzogranite with K-feldspar megacrysts; internally massive, intense contact-parallel foliation with down-dip mineral lineation.|05-AUG-15
24684|Bali Monzogranite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2676 +/- 8 Ma - 2667 +/- 3 Ma (isotopic).||||Coarse-grained monzogranite with K-feldspar megacrysts; internally massive, intense contact-parallel foliation and local development of protomylonite.|
24684|Bali Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
24684|Bali Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv, 100k_geologysub10_lut.csv.|2676+\-8 Ma; 2667+\-3 Ma||||Coarse-grained monzogranite with K-feldspar megacrysts; internally massive, intense contact-parallel foliation and local development of protomylonite|
24684|Bali Monzogranite|73238|5|Briefly described|p20 Fig.15, 21|||NW of Kalgoorlie, Eastern Goldfields Terrane. Deformation structures briefly descibed.||||||
24684|Bali Monzogranite|73391|6|Mentioned|p297, 300, 304, 316, 347, 350|||A composite batholith; intrusion involved more than one phase.|2676 +/- 8 Ma to 2667 +/- 3 Ma.|||||
29756|Balingup Complex|24168|5|Briefly described|p647|Archean|Archean|||||||07-NOV-08
29756|Balingup Complex|43030|5|Briefly described|Map Legend|||||||||
29756|Balingup Complex|43038|6|Mentioned|p8|||||||||
29756|Balingup Complex|43189|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
29756|Balingup Complex|43212|5|Briefly described|p1,p2.||Archean|||||||07-NOV-08
35671|Ballarat Conglomerate|23142|5|Briefly described|p203 Fig.2|||||||||
35671|Ballarat Conglomerate|63637|5|Briefly described|p12|||A basal unit at Kanowna Belle. Overlain by Kanowna Conglomerate. Geological province: Eastern Goldfields Province. Clasts of feldspar+/-quartz-phyric dacite are present in analysed drillholes.||||||17-OCT-07
35671|Ballarat Conglomerate|70482|5|Briefly described|p319|Archean|Archean|Part of greenstone successions around the Scotia-Kanowna Dome, Eastern Goldfields Superterrane, Eastern Yilgarn Craton.||Kalgoorlie Sequence.||Unconformably overlies Kambalda Sequence units. Is overlain conformably by Ballarat turbidite.|Very poorly sorted and internally massive; dominated by well-rounded feldspar-phyric clasts and angular to subangular ultramafic and high-Mg to basaltic clasts.|
35671|Ballarat Conglomerate|71166|6|Mentioned|p22||||||||Polymictic conglomerate and grit with clasts dominated by mafic and ultramafic rocks.|
35671|Ballarat Conglomerate|72049|6|Mentioned|p259|||Kalgoorlie Terrane.||Black Flag Group||||
35671|Ballarat Conglomerate|73391|5|Briefly described|p51, 146, 157, 187, 239, 304, 443|||See also Appendices. In this study, this name is almost invariably presented (informally) as Ballarat conglomerate or Ballarat conglomerate member. In both forms it is treated as one of three sub-units of the Ballarat member [sic] of the Black Flag Group; possibly of the lower part of the Black Flag Formation.|2695 +/- 6 Ma (MDA).|||Overlies Spargoville Formation. Is overlain gradationally by Kanowna Conglomerate and (unconformably) Grave Dam Grit/member. Time-correlated with White Flag Formation.|Clasts are dominantly ultramafic.|
33908|Ballinooka inlier|22449|6|Mentioned|Table3 P27||Archean|Age of unit is 2900 Ma||||||07-NOV-08
30078|Ballythanna Sandstone Member|14228|5|Briefly described|p8|Permian|Permian|Mory and Backhouse (1997).||Callytharra Formation|||Sandstone indicating river/delta incursion.|
30078|Ballythanna Sandstone Member|23726|5|Briefly described|p12|Early Permian|Early Permian|Of Callytharra Formation. Geological Province: Carnarvon Basin||||||
30078|Ballythanna Sandstone Member|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Light tan fine-grained to medium-grained sandstone 50%; fine-grained sandstone with common carbonaceous flaser interbeds, whisps and slumped layers; pyritic; bioturbated 50%.|05-JAN-23
30078|Ballythanna Sandstone Member|67200|5|Briefly described|p18 table 1, p47, p50, p55, app 2 p5|||Thermal conductivity of 3.36 W/mK||Callytharra Formation|||Fine-medium grained sandstone. Fine grained sandstone with common carbonaceous flaser interbeds, whisps and slumped layers; pyritic; bioturbated.|
30078|Ballythanna Sandstone Member|67977|5|Briefly described|p480, p481 Fig. 2, p482 Fig. 3, p485-7|Artinskian|Sakmarian|Sand prone facies. Fossils rare in this interval of Callytharra Formation. Geol. Prov: Merlinleigh Sub-basin, Southern Carnarvon Basin. See Ballythanna Sandstone.||Callytharra Formation|||Sandstone.|18-SEP-14
30078|Ballythanna Sandstone Member|72910|4|Described|p4-5, p7, p16-17, p21-23, p30.|Artinskian|Sakmarian|Thickness <300m. Restricted to the Byro Sub-basin. Type section in Ballythanna 1, 65-298 m. Depositional environment: lower delta plain or tidal channel, from enclosing sediments and acritarchs. See also p32-33, p39-42.||Callytharra Formation|||Fine to medium-grained, clean, cross-bedded sandstone grading into carbonaceous and bioturbated quartz sandstone.|
30078|Ballythanna Sandstone Member|73117|6|Mentioned|p15|Artinskian|Sakmarian|||Callytharra Formation||||
30078|Ballythanna Sandstone Member|73623|6|Mentioned|p16|||"Merlinleigh Basin. The rank (Member) is not stated; the unit is ""designated within the formation"". Represents a progradational phase with the influx of quartz sand."||Callytharra Formation||||
75361|Balpe Lakes Monzogranite|66113|5|Briefly described|Map legend|Archean|Archean|Yilgarn Craton. Age shown as c.2643 Ma. Monzogranite; fine- to medium-grained, equigranular; massive to weakly foliated; margins may be strongly foliated.||||||
75361|Balpe Lakes Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton. U/Pb SHRIMP magmatic crystallization age. See geochron file 193361.1.pdf, 193360.1.pdf (2010).|2643+/-8 Ma|||Intrudes Hope Campbell Orthogneiss.|Monzogranite; fine to medium-grained, equigranular; massive to weakly foliated; margins may be strongly foliated.|05-AUG-15
75361|Balpe Lakes Monzogranite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|See also 100k_geologyp14_lut.csv and 500k_interpgeop14_lut.csv. Age derived from monzogranite sample (193361.1.pdf).|2643 Ma +/- 8 Ma (SHRIMP)||||Monzogranite; fine to medium-grained, equigranular; massive to weakly foliated; margins may be strongly foliated.|
75361|Balpe Lakes Monzogranite|70802|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism.|2643+\-8 Ma||||Monzogranite; fine to medium-grained, equigranular; massive to weakly foliated; margins may be strongly foliated|
75361|Balpe Lakes Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). Sample GSWA 193361 (metamonzogranite) yielded a weighted mean 207Pb/206Pb date of 2643+\-8 Ma, interpreted to be magmatic crystallisation age of themonzogranite. See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 100k_geologyp14_lut.csv, 500k_interpgeop_lut.csv, 100k_geologysub14_lut.csv, 2_5m_interpgeop15_lut.csv.|2643+\-8 Ma||||Monzogranite; fine to medium-grained, equigranular; massive to weakly foliated; margins may be strongly foliated|
75361|Balpe Lakes Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||2643+/-8 Ma.||||Monzogranite; fine to medium-grained, equigranular; massive to weakly foliated; margins may be strongly foliated.|
74593|Balwina Granite|64277|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Muscovite and biotite monzogranite; locally porphyritic; minor biotite granodiorite; highly magnetic.||||||29-JUL-08
74593|Balwina Granite|66129|5|Briefly described|p213, p214, p215 Fig.2|Statherian|Statherian|100 sq. km, continuous ellipsoidal shape. In Frederick Suite. 1795 Ma. Fine to medium grained, even-textured to seriate granodiorite to monzogranite.||||||
74593|Balwina Granite|66468|6|Mentioned|p17 Fig.3, p18 Fig.5, p25 Fig.8|||||||||
74593|Balwina Granite|68474|6|Mentioned|p573|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen.|ca. 1795 Ma||||Monzogranite., granodiorite.|
74593|Balwina Granite|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleoproterozoic|Paleoproterozoic|See also 100k_maginterpgeop_lut.csv, and GEOCHRON. Granites-Tanami Complex. Low gravity; non- to highly magnetic.|1857 +/- 18 Ma (Wingate et al., 2009).|Frederick Suite||Intrudes Killi Killi and Stubbins Formations.|Muscovite and biotite monzogranite; locally porphyritic; minor biotite granodiorite|
74593|Balwina Granite|69253|5|Briefly described|p759, p760 Fig.14, p761, p766|||Petrophysical properties described.||Unit in Frederick Suite.||||
74593|Balwina Granite|69587|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Geological province: Granites-Tanami Orogen, North Australian Craton. Events: Alice Springs Orogeny; Tanami Orogeny D1t. Sample GSWA 178860 (foliated biotite monzogranite) yielded a discordia regression with an upper intercept date of 1857+\-18 Ma, interpreted as the magmatic crystallisation age of the granite. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|1835-1795 Ma (inferred)|||Intrudes into Killi Killi Formation and Stubbins Formation.|Muscovite and biotite monzogranite; locally porphyritic; minor biotite granodiorite; highly magnetic|
74593|Balwina Granite|70142|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|1835-1795 Ma.||||Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite.|
74593|Balwina Granite|70143|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.||||||
74593|Balwina Granite|70826|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|Intruded during intracratonic reactivation of the Capricorn Orogen.||||||
74593|Balwina Granite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. Age inferred.|||||Muscovite and biotite monzogranite; locally porphyritic; minor biotite granodiorite; highly magnetic.|
74593|Balwina Granite|73089|4|Described|p3, p8-9, p13, p20-21, p23, p38, p44|Orosirian|Orosirian|Granites-Tanami Orogen. 9 x 5 km ovoid intrusion about 39 km west-northwest of Coyote. [See report for geochon details from three samples]. May be associated with the 1810-1790 Ma Stafford Event.|1807-1800 Ma|Frederick Suite|||Generally seriate-textured, medium grained monzogranites to granodiorites.|
36838|Bamboo Creek Member|23570|5|Briefly described|p68|Archean|Archean|Of Hardey Formation.  See also Bamboo Creek Porphyry of Noldart & Wyatt (1962).   Age: 2756+/-8Ma (SHRIMP U-Pb).  Geological Province: Pilbara Craton.||||||22-OCT-15
36838|Bamboo Creek Member|23575|5|Briefly described|Map Legend|Archean|Archean|Of Hardey Formation.||||||07-NOV-08
36838|Bamboo Creek Member|23583|5|Briefly described|Map Legend|Archean|Archean|Of Hardey Formation. Underlain by Koongaling Volcanic Member. Geological Province: Hamersley Basin.||||||07-NOV-08
36838|Bamboo Creek Member|23585|4|Described|p15|Archean|Archean|Age: c.2756+/-8 Ma (SHRIMP zircon). Previously Bamboo Creek Porphyry. Of Hardey Formation. Overlain by Kylena Formation. Underlain by Mount Roe Basalt. Geological Province: Hamersley Basin.||||||07-NOV-08
36838|Bamboo Creek Member|23783|5|Briefly described|p85 Fig. 49|Archean|Archean|Of Fortescue Group.||||||07-NOV-08
36838|Bamboo Creek Member|44229|5|Briefly described|Map legend|Archean|Archean|Of the Hardey Formation.  Massive and flow-banded porphyry, porphyry breccia and bedded tuffaceous rocks, and quartz-feldspar and feldspar porphyry.  Age: c.2756Ma.||||||07-NOV-08
36838|Bamboo Creek Member|50189|3|Fully described|p21|Archean|Archean|Supersedes the Bamboo Creek Porphyry. Of the Hardey Formation. A felsic porphyry complex. Age: 2756 +/- 8Ma. See also p10 Table 1.||||||07-NOV-08
36838|Bamboo Creek Member|50287|5|Briefly described|Map Legend|Archean|Archean|Of Hardey Formation. Geological Province: Hamersley Basin. Quartz-feldspar porphyry; commonly columnar jointed, locally layered.||||||07-NOV-08
36838|Bamboo Creek Member|50381|5|Briefly described|Map Legend|Archean|Archean|Of Hardey Formation (Fortescue Group). Geological Province: Hamersley Basin, Pilbara Craton. Age: c. 2756 Ma.||||||08-DEC-08
36838|Bamboo Creek Member|50544|3|Fully described|p45-46, p19 Tb. 2 (amended)|Archean|Archean|Of the Hardey Formation (in Oakover Syncline area).  Consists of porphyritic, amygdaloidal, massive, fine-grained and flow-banded rhyolite, rhyodacite and dacite flows.  Age: 2756+/-8Ma (U-Pb zircon, Arndt et al, 1991).||||||07-NOV-08
36838|Bamboo Creek Member|50555|5|Briefly described|Map legend|Archean|Archean|Of the Hardey Formation (Fortescue Group, Mount Bruce Supergroup).  Massive and flow-banded felsic porphyry, porphyry breccia, bedded tuffaceous rock and quartz-feldspar and feldspar porphyry subvolcanic intrusions.  Geol. Province: Hamersley Basin.||||||07-NOV-08
36838|Bamboo Creek Member|60429|4|Described|p20 Fig. 5, p21|Archean|Archean|Of the Fortescue Group. Formerly called Bamboo Creek Porphyry but recent studies have led to revision of lithology. Age: 2756+/-8Ma (SHRIMP U-Pb, Arndt et al, 1991). Max. thickness: 500m in Helen Well area. Detailed lithology included.||||||07-FEB-11
36838|Bamboo Creek Member|60635|6|Mentioned|p51 Fig. 2.2A|||||||||
36838|Bamboo Creek Member|63417|5|Briefly described|Map legend|Archean|Archean|Of Hardey Fm (Fortescue Gp, Mount Bruce Supergp). Age: c.2766Ma. Geol.prov: Fortescue Basin. Rhyolite, rhyodacite and dacite in flows and subvolcanic intrusions; alkali feldspar and quartz phenocrysts; volcanic breccia, welded ignimbrite + lapilli.....||||||07-NOV-08
36838|Bamboo Creek Member|63420|5|Briefly described|Map legend|Archean|Archean|Of Hardey Gp (Fortescue Gp (Mount Bruce Supergp). Age: c.2764-2756Ma. Geological Province: Marble Bar Sub-basin/Hamersley Basin. Porphyritic dacite, rhyodacite and rhyolite; coarse- to fine-grained alkali feldspar and quartz phenocrysts; locally as dykes.||||||07-NOV-08
36838|Bamboo Creek Member|64621|5|Briefly described|Map legend|Archean|Archean|Of Hardey Formation (Fortescue Group). Porphyritic dacite, rhyodacite and rhyolite; coarse- to fine-grained alkali feldspar and quartz phenocrysts; locally as dykes.||||||07-NOV-08
36838|Bamboo Creek Member|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Hardey Formation. Age: c. 2766Ma. Geological Province: Pilbara Craton. Porphyritic rhyodacite with quartz phenocrysts, extrusive in part.||||||07-FEB-11
36838|Bamboo Creek Member|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Hardey Formation. Age: 2766-2752Ma. Geological Province: Hamersley Basin. Fine-grained rhyolitic volcaniclastic siltstone.||||||
36838|Bamboo Creek Member|64936|5|Briefly described|map legend|Archean|Archean|Of Hardey Formation. Rhyolite. Geol. Prov: Hamersley Basin, Pilbara Craton.||||||
36838|Bamboo Creek Member|65008|4|Described|p7, p8 Fig.5, p22, p23, p41|Neoarchean|Neoarchean|Hamersley Basin. Age constrained by the parent Hardey Formation. U-Pb zircon ages (Pidgeon, 1988; Arndt et al., 1991). Previously referred to as the Spinaway Porphyry.|2768 +/- 16 Ma - 2756 +/- 8 Ma|Of the Hardey Formation|||Porphyritic rhyodacite with quartz phenocrysts; extrusive in part.|14-MAY-14
36838|Bamboo Creek Member|65724|5|Briefly described|map legend|Neoarchaean|Neoarchaean|Of Hardey Formation. Rhyolite, rhyodacite, dacite flows/intrusions; volcanic breccia, welded ignimbrite, accretionary lapilli; resedimented pyroclastic deposits. Age: c. 2766 Ma (geochron. D.R. Nelson in prep). Geol. Prov: Hamersley Basin, Pilbara Craton.||||||
36838|Bamboo Creek Member|65726|5|Briefly described|Map legend|Archean|Archean|Hamersley Basin, Pilbara Craton. Mapped as three sub-units.|c.2766 Ma (Wyatt et al. 2001).|Of Hardey Formation.|||Porphyritic and aphanitic rhyolite, rhyodacite and dacite in flows and subvolcanic intrusions and minor volcanic breccia and welded ignimbrite; fine-grained, spherulitic rhyolite dykes; porphyritic rhyolite, rhyodacite and dacite dykes.|
36838|Bamboo Creek Member|65727|5|Briefly described|Map legend|Neoarchean|Neoarchean|Fortescue Basin. Mapped as two sub-units.|2765 - 2760 Ma.|Of Hardey Formation.|||Rhyolite, rhyodacite and dacite in flows and subvolcanic intrusions, volcanic breccia and welded ignimbrite, alkali feldspar and quartz phenocrysts, resedimented pyroclastic deposits; porphyritic rhyolite, rhyodacite and dacite, locally as dykes.|
36838|Bamboo Creek Member|65825|5|Briefly described|p6, p7 Fig.4, p21. |Archean|Archean|Much of the outcrop is deeply weathered. Contacts with Hardey Formation are locally discordant, suggesting that the porphyry may be locally intrusive.||Unit in Hardey Formation.|||A dark green-grey rock crowded with phenocrysts of pinkish (?K-)feldspar and quartz in a fine-grained groundmass; typically massive; possible columnar jointing locally.|
36838|Bamboo Creek Member|65827|3|Fully described|p12 Tb.3, p14 Tb.4, p32-35|Neoarchean|Neoarchean|Thorne and Trendall (2001); cf Bamboo Creek Porphyry (Noldart and Wyatt, 1962). Of Hardey Formation (Fortescue Group). 2766 +/- 7 Ma to 2760 +/- 4 Ma; both SHRIMP U-Pb zircon (Nelson 2005). Coeval with Koongaling Volcanic Member, Gregory Granitic Complex. Shown as equivalent to part of Nullagine Supersequence. Unconformably overlies Mount Roe Basalt; intrudes Mount Edgar Granitic Complex and Mount Roe Basalt. Effusive and explosive eruptions, including synvolcanic intrusions: dark grey to black, porphyritic rhyolite, rhyodacite and dacite. Up to 2000m thick.||||||
36838|Bamboo Creek Member|65828|5|Briefly described|Map legend|Archean|Archean||c.2765 Ma.|Unit in Hardey Formation.|||Quartz-feldspar porphyry; commonly columnar jointed; locally layered.|
36838|Bamboo Creek Member|65829|3|Fully described|p7 Fig.3, p10, pp16-17. |Neoarchean|Neoarchean|Formerly Bamboo Creek Porphyry (Noldart and Wyatt 1962); renamed by Thorne and Trendall (2001). Effusive and explosive eruptions, including synvolcanic intrusions. Exposed as three lenticular bodies. A number of dykes of similar lithology intrude the Mount Roe Basalt and Elsie Creek Tonalite.|c.2766 - 2760 Ma.|Unit in Hardey Formation.|||Red-brown weathering, dark-grey to black, fine- to coarse-grained, porphyritic rhyolite, rhyodacite and dacite; phenocrysts of quartz, sodic plagioclase, orthoclase; local welded ignimbrite, volcanic breccia and accretionary lapilli.|
36838|Bamboo Creek Member|66108|5|Briefly described|Map legend|Neoarchean|Neoarchean|Unit in Hardey Formation. c.2766 Ma. Rhyolite, rhyodacite, and dacite in flows and subvolcanic intrusions; alkali feldspar and quartz phenocrysts; volcanic breccia, welded ignimbrite, with accretionary lapilli; resedimented pyroclastic deposits.||||||
36838|Bamboo Creek Member|66217|4|Described|pp46-47, p55.|Neoarchean|Neoarchean|Fortescue Basin.|2768-2756 Ma (Pidgeon 1984; Arndt et al. 1991).|Unit in Hardey Formation.||Intrudes Carlindi Granitoid Complex.|Rhyolite lavas, and dykes of flow-banded rhyolite; apple-green weathering colour; scattered quartz phenocrysts.|
36838|Bamboo Creek Member|67201|4|Described|p29 Fig.15|||In northern Pilbara Craton, Northern Fortescue Basin, Northeast Pilbara Sub-basin.||Hardey Formation||||
36838|Bamboo Creek Member|68283|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Marble Bar Sub-basin, Fortescue Basin. Age inferred from parent unit.||Of the Hardey Formation.|||Porphyritic dacite, rhyodacite, and rhyolite; coarse- to fine-grained alkali feldspar and quartz phenocrysts; locally as dykes.|07-JAN-15
36838|Bamboo Creek Member|69012|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.|c. 2766 Ma (Blake et al., 2004)|Hardey Formation.|||Rhyolite, rhyodacite, and dacite in flows and subvolcanic intrusions; alkali feldspar and quartz phenocrysts; volcanic breccia, welded ignimbrite, with accretionary lapilli; resedimented pyroclastic deposits|26-OCT-15
36838|Bamboo Creek Member|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|Age derived from sample of porphyritic rock (169037.1.pdf)|2766 +/- 7 Ma (SHRIMP)|Hardey Formation|||Rhyolite, rhyodacite, and dacite in flows and subvolcanic intrusions; alkali feldspar and quartz phenocrysts; volcanic breccia, welded ignimbrite, with accretionary lapilli; resedimented pyroclastic deposits|
36838|Bamboo Creek Member|69299|6|Mentioned|p15||||c. 2760 Ma (Pidgeon, 1984; Arndt et al., 1991)|Hardey Formation.||||30-JUN-14
36838|Bamboo Creek Member|69301|5|Briefly described|p18 Fig.7|||Pilbara Craton. Fortescue Basin. Northeast Pilbara Sub-basin.||Hardey Formation||||
36838|Bamboo Creek Member|69590|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Of Northeast Pilbara Sub-basin; Marble Bar Sub-basin, Fortescue Basin. Events: Pilbara Craton breakup. Sample GSWA 169037 (feldspar-quartz porphyry) yielded an interpreted igneous crystallisation age of 2766+\-7 Ma for the porphyry (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 250k_interpgeol_lut.csv.|2766-2749 Ma (isotopic; inferred)|Unit of Hardey Formation.|||Rhyolite, rhyodacite, and dacite in flows and subvolcanic intrusions; alkali feldspar and quartz phenocrysts; volcanic breccia, welded ignimbrite, with accretionary lapilli; resedimented pyroclastic deposits|
39605|Bamboo Springs Monzogranite|24531|5|Briefly described|p29, p8-9 Fig. 3|Archean|Archean|Of the Shaw Granitoid Complex. Well-foliated, coarse-grained, biotite monzogranite with elongate, rectangular K-feldspar phenocrysts.||||||15-APR-13
39605|Bamboo Springs Monzogranite|24532|5|Briefly described|Map legend|Archean|Archean|Of the Shaw Granitoid Complex.||||||07-NOV-08
39605|Bamboo Springs Monzogranite|50381|5|Briefly described|Map Legend|Archean|Archean|Of Shaw Granitoid Complex. Geological Province: Pilbara Craton.||||||07-NOV-08
39605|Bamboo Springs Monzogranite|50427|5|Briefly described|p187 Fig.8|Archean|Archean|Age: ?3310 Ma. Of Shaw Granitoid Complex.||||||07-NOV-08
39605|Bamboo Springs Monzogranite|63441|5|Briefly described|p12 tb. 2, p38|Archean|Archean|Of Cutinduna Supersuite. Age: 2908 +/-5 Ma. Geological province: Pilbara Craton. Part of the Shaw Granitic Complex. Coarsely K-feldspar porphyritic monzogranite with a strong synmagmatic foliation defined by aligned K-feldspar phenocrysts.||||||15-APR-13
39605|Bamboo Springs Monzogranite|64654|5|Briefly described|Map Legend|Archaean|Archaean|Of Cutinduna Supersuite. Age: c. 2908 Ma. Geological Province: Pilbara Craton. Biotite monzogranite, K-feldspar porphyritic; coarse grained; magmatic foliation.||||||15-APR-13
39605|Bamboo Springs Monzogranite|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Cutinduna Supersuite. Age: c. 2908 Ma. Geological Province: Pilbara Craton. Biotite monzogranite; K-feldspar porphyritic; coarse grained; magmatic foliation.||||||15-APR-13
39605|Bamboo Springs Monzogranite|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Shown as the only unit in Cutinduna Supersuite. c. 2908 Ma. Biotite monzogranite; K-feldspar porphyritic; coarse-grained; magmatic foliation.||||||15-APR-13
39605|Bamboo Springs Monzogranite|68282|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|c.2908 Ma|Of the Cutinduna Supersuite|||Biotite monzogranite; K-feldspar porphyritic; coarse grained; magmatic foliation.|
39605|Bamboo Springs Monzogranite|69012|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|c. 2908 Ma|Of the Cutinduna Supersuite.|||Comprises biotite monzogranite; K-feldspar porphyritic; coarse grained; magmatic foliation.|15-AUG-18
39605|Bamboo Springs Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Cutinduna Supersuite|||Biotite monzogranite; K-feldspar porphyritic; coarse grained; magmatic foliation.|
39605|Bamboo Springs Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; Mosquito Creek Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|2908 Ma (isotopic)|Unit of Cutinduna Supersuite.|||Biotite monzogranite; K-feldspar porphyritic; coarse grained; magmatic foliation|
39605|Bamboo Springs Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
39605|Bamboo Springs Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||2927+/-10 Ma|Sisters Supersuite|||Biotite monzogranite; K-feldspar porphyritic; coarse grained; magmatic foliation.|
39605|Bamboo Springs Monzogranite|72668|5|Briefly described|p16, p22, p29|||Shaw Granitic Complex, East Pilbara. Contains a strong, parallel, syn-magmatic foliation.|2908 +/- 5 Ma|Cutinduna Supersuite||||12-JAN-22
36845|Bandalup Ultramafics|23727|4|Described|p7|||Overlying unit Maydon Basalt. Geological Province: Carlingup Terrane. Max. thickness: 1500 m.||||||
36845|Bandalup Ultramafics|23728|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Maydon Basalt. Underlying unit Chester Formation. Geological Province: Yilgarn Craton.||||||07-NOV-08
36845|Bandalup Ultramafics|23752|4|Described|p4|Archean|Archean|Geological Province: Carlingup Terrane.||||||07-NOV-08
36845|Bandalup Ultramafics|23754|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Maydon Basalt. Underlying unit Chester Formation. Geological Province: Yilgarn Craton.||||||07-NOV-08
36845|Bandalup Ultramafics|64580|4|Described|map legend|Archean|Archean|Metamorphosed komatiitic basalt and pyroxenite; minor high-Mg basalt; tremolite and talc-rich schist.||||||15-DEC-08
36845|Bandalup Ultramafics|65487|5|Briefly described|p6|||Overlies the Chester Formation and underlies the Maydon Basalt in the Carlingup Greenstone Belt. Consists of metamorphosed komatiites with minor high-Mg metabasalt and metagabbro, interlayered with thin units of metamorphosed BIF. 1.5 km thick.||||||10-FEB-14
36845|Bandalup Ultramafics|69404|5|Briefly described|p10, p10 Fig.11|||Carlingup Terrane.||||Faulted against the underlying Chester Formation. Overlain by the Maydon Basalt.|Komatiite; olivine orthocumulate and spinifex textured flows; minor komatiitic basalt and chemical metasedimentary rocks (banded iron formation, chert and massive pyrite).|
36845|Bandalup Ultramafics|69559|5|Briefly described|500k_geologyp08_lut.csv|Archean|Archean||||||Metamorphosed komatiitic basalt and pyroxenite; minor high Mg basalt; tremolite and talc rich schist.|
36845|Bandalup Ultramafics|70156|4|Described|500k_interpgeop14_lut.csv|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Youanmi Terrane events (3200-2600 Ma).|3200-2958 Ma (inferred)||||Metamorphosed komatiitic basalt and pyroxenite; minor high-Mg basalt; tremolite- and talc-rich schist|
36845|Bandalup Ultramafics|70794|4|Described|500k_interpgeop14_lut.csv|Mesoarchean|Mesoarchean||3200-2958 Ma inferred.||||Metamorphosed komatiitic basalt and pyroxenite; minor high-Mg basalt; tremolite and talc rich schist.|
36845|Bandalup Ultramafics|70802|5|Briefly described|500k_interpgeop14_lut.csv|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Youanmi Terrane events.|3200-2958 Ma (inferred)||||Metamorphosed komatiitic basalt and pyroxenite; minor high-Mg basalt; tremolite- and talc-rich schist|
36845|Bandalup Ultramafics|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Youanmi Terrane.|||||Metamorphosed komatiitic basalt and pyroxenite; minor high-Mg basalt; tremolite- and talc-rich schist.|
34708|Bandicoot Range beds|22754|5|Briefly described|p11 Tb. 3|Mesoproterozoic|Mesoproterozoic|Of Carr Boyd Group.||||||
34708|Bandicoot Range beds|44155|5|Briefly described|p250 Tb.3-10|||1035m thick. Stratigraphic position unknown.||Carr Boyd Group|||Quartz and argillaceous sandstone, and conglomerate, interbeds ferruginous sandstone, minor red shale and fine micaceous sandstone.|
34708|Bandicoot Range beds|71267|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Carr Boyd Group.|||Quartz sandstone, conglomerate, ferruginous sandstone, siltstone and shale|
34951|Bangemall Supergroup|22897|6|Mentioned|102|||Geol province: Bangemall Basin.||||||08-SEP-08
34951|Bangemall Supergroup|22905|4|Described|p51|Mesoproterozoic|Mesoproterozoic|Supersedes the Bangemall Group.||||||
34951|Bangemall Supergroup|23403|6|Mentioned|p5|||Formerly Bangemall Group.||||||
34951|Bangemall Supergroup|23485|4|Described|p30|Mesoproterozoic|Paleoproterozoic|Formerly Bangemall Group.||||||07-NOV-08
34951|Bangemall Supergroup|23486|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
34951|Bangemall Supergroup|23487|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
34951|Bangemall Supergroup|23525|4|Described|p28||Statherian|Previously named "Bangemall Group". Age: <1640Ma. Geological Province: Bangemall Basin.||||||22-MAY-08
34951|Bangemall Supergroup|23527|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|In the Edmund Basin.||||||08-SEP-08
34951|Bangemall Supergroup|23529|5|Briefly described|p7|||Geological Province: Bangemall Basin||||||
34951|Bangemall Supergroup|23620|6|Mentioned|p3|||||||||
34951|Bangemall Supergroup|23774|5|Briefly described|p731|Mesoproterozoic|Paleoproterozoic|Underlying unit: Ashburton Formation - unconformable.||||||07-NOV-08
34951|Bangemall Supergroup|23780|5|Briefly described|p13|Proterozoic|Proterozoic|||||||
34951|Bangemall Supergroup|23781|5|Briefly described|p62|||||||||
34951|Bangemall Supergroup|24017|5|Briefly described|p21||Paleoproterozoic|Formerly Bangemall Group.||||||07-NOV-08
34951|Bangemall Supergroup|24025|5|Briefly described|p15|||Geological Province: Collier Basin.||||||
34951|Bangemall Supergroup|24110|5|Briefly described|Plate 1|Proterozoic|Proterozoic|Geological Province: Collier Basin||||||
34951|Bangemall Supergroup|24115|4|Described|p1, p2|Mesoproterozoic|Mesoproterozoic|Overlain by the Sunbeam Group. Geological Province: Edmund and Collier Basins. Formerly of Group status (Muhling and Brakel, 1985).||||||
34951|Bangemall Supergroup|24183|2|Defined|p1, p2 Fig.1, p6|Stenian|Mesoproterozoic|Formerly known as Bangemall Group. Age: ~1100 Ma. Unconformably overlies the Gascoyne Complex, Wyloo, Bresnahan and Mount Minnie Groups.||||||
34951|Bangemall Supergroup|24332|5|Briefly described|p135 Fig. 1|Mesoproterozoic|Mesoproterozoic|Age: <1620Ma.||||||
34951|Bangemall Supergroup|24535|4|Described|p2|Mesoproterozoic|Mesoproterozoic|Comprises Edmund Group and Collier Group. Unconformably overlain by the Sunbeam Group. Contains large tholeiitic dolerite sills.||||||
34951|Bangemall Supergroup|24544|4|Described|p6|Mesoproterozoic|Mesoproterozoic|Age: <1640 Ma. Unconformably overlies Wyloo, Capricorn, Mount Minnie and Bresnahan Groups, and Mount James Formation. Max. thickness: 10 km. Mostly fine grained siliciclastic and carbonate rocks.||||||24-JUN-13
34951|Bangemall Supergroup|24607|5|Briefly described|p968 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age stated to be: 1638 +/- 14 Ma.||||||30-NOV-10
34951|Bangemall Supergroup|50008|5|Briefly described|p43|Mesoproterozoic|Mesoproterozoic|Unconformably overlain by Tarcunyah Group.||||||
34951|Bangemall Supergroup|50010|5|Briefly described|p53, 54|Mesoproterozoic|Mesoproterozoic|Mainly lower greenschist facies, fine grained siliciclastic and carbonate rocks.||||||24-JUN-13
34951|Bangemall Supergroup|50188|5|Briefly described|p2, p10 Fig. 3|||Includes Collier and Scorpion Groups. Superseded Bangemall 'Group'.  Geological Province: Bangemall Basin.||||||16-JUL-08
34951|Bangemall Supergroup|50195|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes the Salvation and Scorpion Groups.||||||
34951|Bangemall Supergroup|50216|5|Briefly described|p202|Mesoproterozoic|Mesoproterozoic|Geological Province: Edmund and Collier Basins.||||||13-JAN-05
34951|Bangemall Supergroup|50218|5|Briefly described|p238 Fig. 1|Mesoproterozoic||Age: <1640Ma. See also p242 Fig. 4.||||||07-FEB-11
34951|Bangemall Supergroup|50219|5|Briefly described|p258 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: <1640Ma.||||||07-FEB-11
34951|Bangemall Supergroup|50221|5|Briefly described|p312|Mesoproterozoic|Paleoproterozoic|Max. age: 1638+/-14 Ma.||||||07-NOV-08
34951|Bangemall Supergroup|50225|3|Fully described|p385, p386 Fig. 1|Mesoproterozoic|Mesoproterozoic|Supersedes Bangemall Group. Subdivided into older Edmund Gp + younger Collier Gp. Unconformably overlies Gascoyne Complex. Max. age: <1629Ma; min age:c.1070Ma. Geological Province: Edmund and Collier Basins.||||||07-FEB-11
34951|Bangemall Supergroup|50226|5|Briefly described|p424 Fig. 5, p426|||Includes Edmund, Collier and Scorpion Groups.  Age: 1.07Ga.  Geological Province:  Bangemall Basin.||||||09-DEC-04
34951|Bangemall Supergroup|50228|5|Briefly described|p482, p492|Mesoproterozoic|Mesoproterozoic|Siltstone, shale, carbonate, chert and sandstone. Unconformably overlain by Tarcunyah Group.||||||
34951|Bangemall Supergroup|50292|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Geological Provinces: Edmund and Collier Basins.||||||07-NOV-08
34951|Bangemall Supergroup|50312|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Geological Province: Edmund Basin.||||||07-NOV-08
34951|Bangemall Supergroup|50313|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Geological Province: Edmund Basin.  Includes: Edmund Group.||||||07-NOV-08
34951|Bangemall Supergroup|50334|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Bangemall Superbasin||||||11-JUN-04
34951|Bangemall Supergroup|50380|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Geological Province: Edmund Basin.||||||07-NOV-08
34951|Bangemall Supergroup|60301|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes: Collier Group, Edmund Group. Geological Province: Collier Basin, Edmund Basin.||||||17-AUG-04
34951|Bangemall Supergroup|60470|6|Mentioned|p2, 5, 8|Mesoproterozoic|Mesoproterozoic|||||||
34951|Bangemall Supergroup|60535|5|Briefly described|p555, 556 Fig.1|Mesoproterozoic|Mesoproterozoic|Includes: Edmund Group, Collier Group, Manganese Group.||||||
34951|Bangemall Supergroup|61262|6|Mentioned|p458 App.|Mesoproterozoic|Mesoproterozoic|Includes the Edmund Group. Overlies the Durlacher Supersuite. See also p445. ||||||
34951|Bangemall Supergroup|61732|5|Briefly described|p84, p130|Mesoproterozoic|Mesoproterozoic|Age: 1.70 - 1.620Ga. Geological Province: Bangemall Basin.||||||07-FEB-11
34951|Bangemall Supergroup|61850|5|Briefly described|p323, p324 Fig. 1|Proterozoic|Proterozoic|Includes the Collier Group. Dominantly siliciclastc sedimentary rocks, ranging from conglomerate through to shale and mudstone. Overlies the Gascoyne Complex rocks. In the Capricorn Orogen.||||||03-JUL-06
34951|Bangemall Supergroup|62986|5|Briefly described|p18|Mesoproterozoic|Mesoproterozoic|Contains mafic sills and dykes.||||||
34951|Bangemall Supergroup|63022|6|Mentioned|p1018, p1019|||Contains mafic sill complexes.||||||01-FEB-12
34951|Bangemall Supergroup|63246|5|Briefly described|p478 Fig. 1|Mesoproterozoic|Mesoproterozoic|Includes Collier and Edmund Groups. Overlies Gascoyne Complex.||||||24-JUN-13
34951|Bangemall Supergroup|63417|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the Manganese Group. Age: 1465-1070Ma. Geological Province: Collier Basin.||||||23-JUL-07
34951|Bangemall Supergroup|63469|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Includes Edmund Group.||||||24-SEP-07
34951|Bangemall Supergroup|63470|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Includes the Edmund Group. Age: <1620Ma. Geological Province: Edmund Basin.||||||07-NOV-08
34951|Bangemall Supergroup|63866|5|Briefly described|p162-p163|||Presumably obsolete [as the author uses the 'former Bangemall Supergroup' on p162].|c. 1620 Ma||Includes the Scorpion and Salvation Groups.|||
34951|Bangemall Supergroup|63869|4|Described|p1, p20, p24, p27-29, p32, p42-43, p44|Mesoproterozoic|Paleoproterozoic|See also p45, p46-48, p49, p51-53, p59-60. Formerly Bangemall Series, series, Beds and beds (Maitland, 1909): all four appear in his account. Subsequently Bangemall Group (Halligan and Daniels, 1964; Daniels, 1967). Stratigraphy revised by Muhling and Brakel (1985). Recognition of a significant regional unconformity between Edmund and Collier Subgroups (Cooper et al., 1998) led to their elevation to Group status and this unit to Supergroup status (Martin et al.,1999; Martin and Thorne, 2002). Deformed by 1070-755 Ma Edmundian Orogeny. A variety of mineral deposits is described.|> c.1070 Ma (intrusive rel.). <~1620 (underlying)||Includes Edmund and Collier Groups.|Unconformably overlies Gascoyne Complex, Wyloo and Capricorn Groups.|Siltstone, dololutite, dolarenite, stromatolitic dolostone, sandstone.|07-MAR-18
34951|Bangemall Supergroup|64284|5|Briefly described|p58 Fig. 1|||Includes Scorpion and Collier Groups. Geological Province: Bangemall Basin.||||||07-FEB-11
34951|Bangemall Supergroup|64285|5|Briefly described|p67 Fig. 2|||Includes Scorpion and Collier Groups. Geological Province: Bangemall Basin.||||||07-FEB-11
34951|Bangemall Supergroup|64286|5|Briefly described|p72|||||||||07-FEB-11
34951|Bangemall Supergroup|64287|5|Briefly described|p31, p34 Fig. 2|||Includes Edmund and Collier Groups. Age: 1.64-1.00Ma. Geological province: Jillawarra Sub-basin. Lower section hosts Abra base metal prospect.||||||24-JUN-13
34951|Bangemall Supergroup|64580|6|Mentioned|map legend|||||||||
34951|Bangemall Supergroup|64722|5|Briefly described|p7, p15 Fig. 6, p23|Mesoproterozoic|Mesoproterozoic|Of the 1620 - 1070 Ma Edmund Basin. Sediment thought to be sourced from the West Australian Craton, including Gascoyne Complex and equivalent basins of Capricorn Orogen and southern Pilbara Craton.|||Contains Edmund and Collier Groups.|||11-APR-12
34951|Bangemall Supergroup|64725|5|Briefly described|pp64-67. |Mesoproterozoic|Mesoproterozoic|Edmund Basin. Includes a series of metalliferous sill complexes.||||||
34951|Bangemall Supergroup|64728|4|Described|pp93-96, pp98-99, pp106-109.|Mesoproterozoic|Mesoproterozoic|4-10 km of mostly fine-grained siliciclastic and carbonate sedimentary rocks. Source areas were probably the northern Gascoyne Complex and the Pilbara Craton. Detrital zircon geochronology for several member Formations is detailed.|c.1620-1070 Ma.||Includes Edmund and Collier Groups.|Unconformably overlies Gascoyne Complex to the south, and Wyloo and Capricorn Groups to the north.||
34951|Bangemall Supergroup|64748|6|Mentioned|p276|||?Intruded by sills of the Warakurna Igneous Province||||||
34951|Bangemall Supergroup|64772|5|Briefly described|p5, p13, p19 Fig.9|Mesoproterozoic|Paleoproterozoic|Supersedes Bangemall Group. Presented as Upper and Lower Bangemall Supergroups in Fig. 7, p14 with ages of c.1100Ma and c.1640Ma respectively.|||Includes Salvation Group, Scorpion Group.|||25-NOV-13
34951|Bangemall Supergroup|64777|5|Briefly described|p1-4, p6-8 |Mesoproterozoic|Mesoproterozoic||||Includes the Edmund and Collier Groups.|Unconformably underlies the Tarcunyah Group.||
34951|Bangemall Supergroup|64872|6|Mentioned|p25, p24 Fig.1|Mesoproterozoic|Mesoproterozoic|Includes Edmund and Collier Groups. Sheared and faulted around 570 Ma.||||||
34951|Bangemall Supergroup|65152|5|Briefly described|p2 Fig.1.|Mesoproterozoic|Mesoproterozoic|Includes Edmund and Collier Groups. Unconformably overlies Gascoyne Complex.||||||01-MAY-15
34951|Bangemall Supergroup|65369|5|Briefly described|p35, 36|||Western Australian; includes mafic sill complex. Includes the Glenayle Dolerite.||||||19-APR-13
34951|Bangemall Supergroup|65450|6|Mentioned|p3||||||Edmund Group|||
34951|Bangemall Supergroup|65453|5|Briefly described|map legend|Mesoproterozoic|Paleoproterozoic|Includes Edmund Group. Geol. Prov: Edmund Basin.||||||
34951|Bangemall Supergroup|65472|6|Mentioned|p5 Fig. 4|||Collier and Edmund Basins.|||Collier Group, Scorpion Group|||
34951|Bangemall Supergroup|65506|5|Briefly described|p985-999|c.1070 Ma.|c.1465 Ma.|Contains Edmund and Collier Groups. Capricorn Orogen. Unconformably overlies the Gascoyne Complex in the west and Salvation and Scorpion Groups in the East. Various ages listed. Geochemistry detailed.||||||
34951|Bangemall Supergroup|65545|5|Briefly described|Map Legend|Mesoprotoerozoic|Paleoproterozoic|Edmund Basin. c. 1460 - <1620 Ma. Consists of Edmund Group on this mapsheet.||||||
34951|Bangemall Supergroup|65549|5|Briefly described|Map Legend|Calymmian|Statherian|Includes Edmund Group. Of Edmund Basin. Shown as younger than Durlacher Supersuite of the Gascoyne Province.||||||
34951|Bangemall Supergroup|65692|6|Mentioned|p68|||Affected by the 1030-950 Ma Edmundian Orogeny.||||||
34951|Bangemall Supergroup|65693|6|Mentioned|p8.|||Sill complexes c. 800 km west of the Musgrave Province.||||||
34951|Bangemall Supergroup|65724|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Includes Manganese Group. Sedimentary rocks. Geol. Prov: Collier Basin.||||||
34951|Bangemall Supergroup|65826|6|Mentioned|p3 Fig.1. |Mesoproterozoic|Mesoproterozoic|||||||
34951|Bangemall Supergroup|65829|6|Mentioned|p1, p7 Fig.3.  ||||||Includes Manganese Group.|||
34951|Bangemall Supergroup|65830|4|Described|p4, p9-13, p16, p18-19, p21, p25-27, p38|Mesoproterozoic|Mesoproterozoic|May be a hiatus of 395 m.y. between Edmund and Collier Groups. Intruded by two dolerite suites, of which the older has been dated at around 1465 Ma, and the younger at around 1070 Ma (using SHRIMP U-Pb geochronology). See also Bangemall Group. Deformed by Edmundian Orogeny.|> 1465 Ma||Includes Edmund Group, Collier Group, Irregully Formation, Yilgatherra Formation.|Underlain by the Gascoyne Complex. Unconformably underlain by the Ashburton Formation.||
34951|Bangemall Supergroup|65896|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Comprises Edmund Group (1620 - 1465 Ma) in the Edmund Basin; Collier Group (1211 - 1070 Ma) in the Collier Basin. Intruding dolerite and gabbro sills provide minimum age control. ||||||
34951|Bangemall Supergroup|66104|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Comprises Edmund Group (age shown as 1620 - 1465 Ma) in the Edmund Basin; Collier Group (age shown as 1211 - 1070 Ma) in the Collier Basin; and Narimbunna Dolerite (age shown as c.1465 Ma).||||||
34951|Bangemall Supergroup|66105|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin. Map shows it consisting only of the Edmund Group. Age ranges from <1620 Ma to c.1465 Ma.||||||
34951|Bangemall Supergroup|66107|5|Briefly described|p1, p4-5, p10, p13  |Mesoproterozoic|Mesoproterozoic|Ashburton region.|Between c.1620 and c.1070 Ma.||Includes Collier and Manganese Groups.|Unconformably overlies the Gascoyne Complex.||
34951|Bangemall Supergroup|66110|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin. Includes Edmund Group and Ullawarra Formation. Age ranges from <1620-c.1465 Ma.||||||
34951|Bangemall Supergroup|66112|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund and Collier Basins. Comprises Edmund and Collier Groups, and the Narimbunna Dolerite which intrudes the Edmund Group.||||||
34951|Bangemall Supergroup|66241|5|Briefly described|p1, p2, p4, p10. |||Cut by late-stage brittle-ductile faults and shears and associated quartz veins dated at c.570 Ma.|||Includes Edmund and Collier Groups.|||
34951|Bangemall Supergroup|66299|5|Briefly described|p7, p216, p227, pp324-325.|Mesoproterozoic|Mesoproterozoic|Underwent greenschist to amphibolite metamorphism, granitic magmatism and pegmatite intrusion, and widespread deformation from north-south shortening, during Edmundian Orogeny.|||Includes Edmund Group.|In faulted contact with Biddenew Formation.|Siltstones, sandstones and dolostones.|
34951|Bangemall Supergroup|66427|5|Briefly described|p42, p43 Fig.2, p45, p47    |Mesoproterozoic|Mesoproterozoic|Maximum age of 1645 Ma (Martin and Thorne, 2001).|||Includes Collier, Scorpion and Salvation Groups.|||
34951|Bangemall Supergroup|66526|5|Briefly described|p36.|Proterozoic|Proterozoic|Dolerite sills in the Capricorn Province were produced in the Bangemall Event, ME 18 in the Proterozoic Mafic-Ultramafic Magmatic Event Series.|c.1465 Ma.|||||
34951|Bangemall Supergroup|66574|6|Mentioned|p928|||||||||
34951|Bangemall Supergroup|66579|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin|||Shown as including only the Edmund Group.||Clastic and carbonaceous sediments.|
34951|Bangemall Supergroup|66948|5|Briefly described|p18, p24|Mesoproterozoic|Mesoproterozoic|Late Mesoproterozoic age. Contains Horodyskia williamsii fossils.|1465-1070 Ma.|||||
34951|Bangemall Supergroup|67056|6|Mentioned|p419 Fig.2. |||||||||
34951|Bangemall Supergroup|67128|6|Mentioned|p1|Mesoproterozoic|Mesoproterozoic|||||||
34951|Bangemall Supergroup|67129|6|Mentioned|p8|||Collier Basin.||||||06-SEP-17
34951|Bangemall Supergroup|67136|5|Briefly described|Map legend.||||||Includes Edmund and Collier Groups.|||
34951|Bangemall Supergroup|67183|5|Briefly described|p644, p665|Mesoproterozoic|Mesoproterozoic|Deformed by the ca 900 Ma Edmundian Orogeny.|||Includes Collier Subgroup.|||
34951|Bangemall Supergroup|67202|6|Mentioned|p258|Mesoproterozoic|Mesoproterozoic||||Manganese Group.|||
34951|Bangemall Supergroup|67245|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Edmund Basin.|||Includes Moorarie Supersuite, Edmund and Collier Groups and Narimbunna Dolerite.|||
34951|Bangemall Supergroup|67246|5|Briefly described|Map legend.|Mesoproterozoic|Proterozoic||||Includes Edmund Group and Narimbunna Dolerite.|Overlies nonconformably Moorarie Supersuite.||
34951|Bangemall Supergroup|67247|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Edmund Basin.|<1620 Ma.||Includes Edmund Group.|||
34951|Bangemall Supergroup|67371|5|Briefly described|Map legend.|Proterozoic|Proterozoic||||Includes Edmund Group.|||
34951|Bangemall Supergroup|67374|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Edmund and Collier Basins.|||Includes Edmund and Collier Groups and Narimbunna Dolerite.|||
34951|Bangemall Supergroup|67375|5|Briefly described|p229.|Neoproterozoic|Neoproterozoic|Sill complexes and dykes in the Collier Basin. Included in the Warakurna Supersuite.||||||
34951|Bangemall Supergroup|67888|6|Mentioned|p23, p54, p55, p95|Mesoproterozoic|Paleoproterozoic|Contains WA's largest stratabound lead-silver-copper-gold deposit.|||Includes Edmund Group, Collier Group|||
34951|Bangemall Supergroup|68055|6|Mentioned|p77|||Bangemall Superbasin.|||Scorpion, Collier, Salvation Groups.|||
34951|Bangemall Supergroup|68285|5|Briefly described|Map Legend|Stenian|Statherian|Both Edmund and Collier Basins. Age constrained by age of younger Kulkatharra Dolerite (c. 1070 Ma) and older Mangaroon Orogeny (1677-1619 Ma, Sheppard, 2005 AJES)|c. 1620-1070 Ma||Includes the Edmund Group, Collier Group.|||
34951|Bangemall Supergroup|68286|5|Briefly described|Map Legend|Stenian|Statherian|Both Edmund and Collier Basins. Age constrained by age of younger Kulkatharra Dolerite (c. 1070 Ma) and older Mangaroon Orogeny (1677-1619 Ma, Sheppard, 2005 AJES)|c. 1620 -1070 Ma||Includes Edmund Group, Collier Group.|||
34951|Bangemall Supergroup|68521|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic||||Includes the Edmund Group.|||
34951|Bangemall Supergroup|68522|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin.|<1620 - c.1465 Ma||Includes the Edmund Group.|||
34951|Bangemall Supergroup|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv|Mesoproterozoic|Paleoproterozoic||||Includes Edmund Group, Collier Group|||
34951|Bangemall Supergroup|69010|5|Briefly described|Map Legend|Stenian|Statherian|Edmund and Collier Basins.|1620-1070 Ma||Includes Collier Group and Edmund Group.|||24-APR-14
34951|Bangemall Supergroup|69024|6|Mentioned|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.|||Includes the Edmund Group.|||
34951|Bangemall Supergroup|69027|6|Mentioned|Map Legend|Mesoproterozoic|Paleoproterozoic|Ashburton Basin.|||Includes the Edmund Group.|||
34951|Bangemall Supergroup|69166|6|Mentioned|500k_geologyp08_lut.csv|Mesoproterozoic|Paleoproterozoic||||Includes Uaroo Group, Bangemall Group, Edmund Group|||
34951|Bangemall Supergroup|69167|6|Mentioned|geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic||||Includes Manganese Group|||
34951|Bangemall Supergroup|69185|5|Briefly described|500k_geologyp08_lut.csv||||||Includes Collier Group, Edmund Group, Manganese Group, Salvation Group, Uaroo Group.|||
34951|Bangemall Supergroup|69237|5|Briefly described|p2|Calymmian|Statherian||c.1680 Ma.||Edmund, Collier Groups.|||
34951|Bangemall Supergroup|69538|6|Mentioned|p517 Fig.3|||||||||
34951|Bangemall Supergroup|69546|5|Briefly described|p101-102|Mesoproterozoic|Mesoproterozoic|Geological province: Gascoyne Province.|~1680 Ma|||||
34951|Bangemall Supergroup|69553|6|Mentioned|p51,62,64|Mesoproterozoic|Mesoproterozoic||1465-1070 Ma||Includes Backdoor and Arrow Stag formations.|||
34951|Bangemall Supergroup|69590|5|Briefly described|GEOL_LUT_CSV files||| See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv2_5m_geologyp98_lut.|||Includes Manganese Group.|||
34951|Bangemall Supergroup|69596|6|Mentioned|p12 Fig.7|||Edmund and Collier Basins.|||Edmund, Collier Groups.|||
34951|Bangemall Supergroup|69873|5|Briefly described|p52|Mesoproterozoic|Mesoproterozoic|Contains the 'string of beans' fossil, Horodyskia williamsii; also found in Balfour Subgroup (Tas).|1465-1070 Ma.|||||
34951|Bangemall Supergroup|70127|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.|||Edmund Group.|||
34951|Bangemall Supergroup|70132|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic||||Edmund and Collier Groups.|||
34951|Bangemall Supergroup|70136|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Edmund and Collier Basins.|||Edmund and Collier Groups.|||
34951|Bangemall Supergroup|70138|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Edmund Basin.|||Edmund Group.|||
34951|Bangemall Supergroup|70316|6|Mentioned|p120-121, 123-125|||Warakurna LIP. Other very similar age determinations of sills are given.|1071 +/- 8 Ma.|||||
34951|Bangemall Supergroup|70767|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic||<1679-<1171 Ma.||Edmund, Collier Groups.|||
34951|Bangemall Supergroup|70768|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic||<1679-<1171 Ma.||Edmund, Salvation, Collier Groups.|||
34951|Bangemall Supergroup|70795|6|Mentioned|100k_geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic||1171-1070 Ma||Includes Collier Group, Edmund Group, Coobarra Formation|||
34951|Bangemall Supergroup|70796|6|Mentioned|2_5m_interpgeop15_lut.csv|Mesoproterozoic|Mesoproterozoic|Of the Collier Basin, Capricorn Orogen.|||Includes the Collier Group.|||
34951|Bangemall Supergroup|70826|6|Mentioned|p2, p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic||||Manganese Group, Collier Group, Uaroo Group, Edmund Group, Scorpion Group|||20-APR-20
34951|Bangemall Supergroup|70936|5|Briefly described|p61,74|Mesoproterozoic|Mesoproterozoic|Geological province: Pilbara Craton.|||Includes Collier and Manganese groups, Stag Arrow Formation, Backdoor Formation and Edmund Group.|||
34951|Bangemall Supergroup|71003|6|Mentioned|p74|||Pilbara Craton. [Presumably the current usage of the term Bangemall after the group was raised to supergroup status].|||Includes the Collier Group, Magnanese Group and Edmund Group.|||
34951|Bangemall Supergroup|71042|6|Mentioned|p67|||Includes Collier Group.||||||
34951|Bangemall Supergroup|71158|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||Collier Group.|||
34951|Bangemall Supergroup|71210|6|Mentioned|p136|||||||||
34951|Bangemall Supergroup|71267|6|Mentioned|1M_geologyp12_lut.csv||||||Includes Collier Group.|||
34951|Bangemall Supergroup|71269|4|Described|GEOL_LUT_CSV files|||Geological province: Capricorn Orogen; West Australian Craton. See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv.|||Includes Collier Group, Edmund Group, Scorpion Group.|Intruded by Kulkatharra Dolerite.||
34951|Bangemall Supergroup|71484|5|Briefly described|p122,125|Mesoproterozoic|Latest Proterozoic|Geological province: Of Edmund and Collier basins.|||Includes Edmund and Collier groups.||Six depositional pacakges of silstone, mudstone, sandstone, dolostone, chert and conglomerate.|30-AUG-19
34951|Bangemall Supergroup|71869|6|Mentioned|p3|||Capricorn Orogen.|||Includes the Collier Group and Edmund Group.|||
34951|Bangemall Supergroup|72034|6|Mentioned|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Manganese Group.|||
69024|Bapinmarra Dolerite|60976|6|Mentioned|p22|||See also Bapinmarra dolerite. The granophyric zone of the Bapinmarra Dolerite is considered to be a highly favourable host rock for gold. Geological Province: Yilgarn Craton.||||||24-OCT-06
23358|Baramine Volcanic Member|23570|3|Fully described|p156|Archean|Archean|See also p231 App. 1 and Baramine Member.  Of Jeerinah Formation.  Appendix suggests name has been replaced by Barramine Member; however body of text still refers to Barramine Volcanic Member.  Thickness: 175m.   Geological Province: Pilbara Craton||||||07-NOV-08
23358|Baramine Volcanic Member|23583|5|Briefly described|Map Legend|Archean|Archean|Of Jeerinah Formation. Overlying unit Isabella Member. Underlying unit Kuruna Member. Geological Province Hamersley Basin.||||||07-NOV-08
23358|Baramine Volcanic Member|23585|4|Described|p18|Archean|Archean|Of Jerrinah Formation. Overlying unit Isabella Member. Geological Province: Hamersley Basin. Max. thickness: 400 m.||||||07-NOV-08
23358|Baramine Volcanic Member|23594|5|Briefly described|p9 Fig. 6|Archean|Archean|Of Jeerinah Formation. Geological Province: Hamersley Basin.||||||07-NOV-08
23358|Baramine Volcanic Member|23745|4|Described|p13|Archean|Archean|See also page 7 Fig 5. Of Jeerinah Formation.||||||07-NOV-08
23358|Baramine Volcanic Member|23746|4|Described|p20|Archean|Archean|Of Jeerinah Formation. Geological Province: Hamersley Basin.||||||07-NOV-08
23358|Baramine Volcanic Member|36551|6|Mentioned|p90|||||||||
23358|Baramine Volcanic Member|39697|6|Mentioned|p124|||See also Table 6||||||
23358|Baramine Volcanic Member|41687|5|Briefly described|p95|||||||||
23358|Baramine Volcanic Member|42352|5|Briefly described|p16|||Member of Jeerinah Formation. Note on type area P18.||||||
23358|Baramine Volcanic Member|44152|5|Briefly described|p174, p177|||||Lewin Shale|||Includes felsic, as well as basaltic, lavas and pyroclastic rocks.|
23358|Baramine Volcanic Member|44189|5|Briefly described|Map legend||Archean|||||||07-NOV-08
23358|Baramine Volcanic Member|44190|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
23358|Baramine Volcanic Member|44443|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Of Lewin Shale, Fortescue Group.||||||07-NOV-08
23358|Baramine Volcanic Member|46319|4|Described|p14|Proterozoic|Proterozoic|Of Lewin Shale.  Overlain by Pearana Basalt.  Maximum thickness: 250m.||||||
23358|Baramine Volcanic Member|50544|4|Described|p50-51, p44 Fig. 8|Archean|Archean|Of the Jeerinah F.  Consists of a mixture of bedded vitric, lithic and crystal tuffs, minor accretionary tuff interlayered with volcaniclastic rocks.  Underlies Isabella Member.  Max. thickness: 400m.  Geological Province: Gregory Range Inlier.||||||07-NOV-08
23358|Baramine Volcanic Member|50555|5|Briefly described|Map legend|Archean|Archean|Of the Jeerinah Formation (Fortescue Group, Mount Bruce Supergroup).  Coarse to fine-grained, mafic tuff with local accretionary lapilli, and volcanic agglomerate; thin basalt and andesitic basalt flows.  Geological Province: Hamersley Basin.||||||07-NOV-08
23358|Baramine Volcanic Member|69590|4|Described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Of Northeast Pilbara Sub-basin, Fortescue Basin. Events: Pilbara Craton breakup.|2715-2629 Ma (inferred)|Unit of Jeerinah Formation.|||Basalt and basaltic andesite, and basaltic volcanic sandstone and siltstone; local accretionary lapilli|
33645|Bardsley Formation|50188|2|Defined|p18|Cenozoic|Mesoproterozoic|Overlies Earaheedy Group. Only a few metres thick.  Intrudes Boondawari Formation. Type area in text.||||||19-NOV-08
33645|Bardsley Formation|50195|5|Briefly described|Map Legend|||Poorly sorted sandstone, siltstone and granule conglomerate, local valley-fill deposit.||||||
33645|Bardsley Formation|50334|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
33645|Bardsley Formation|64772|5|Briefly described|p17, p40 Fig. 27|Phanerozoic|Phanerozoic|Poorly sorted, variably ferruginised lithic sandstone + granule conglom. infilling an irregular topography underlying the Earaheedy Group.  In Troy Creek area on south-central RHODES. Age: post-dates Collier Group, pre-dates Oligocene-Eocene duricrust. See also  p32 Fig.20, p46 Fig.33.||||||25-NOV-13
23359|Bare Formation|12491|6|Mentioned|p454 Fig.7|Miocene|Oligocene|Presented in figures as Bare, Trealla and Mandu Formations. Mid Oligocene to Mid Miocene.||||||06-NOV-14
23359|Bare Formation|23726|5|Briefly described|p88|Miocene|Oligocene|Overlying unit Delambre Formation. Underlying unit Trealla Limestone. Geological Province: Carnarvon Basin.||||||
23359|Bare Formation|40617|5|Briefly described|p16|||||||||
23359|Bare Formation|40800|2|Defined|p24|late Miocene|middle Miocene|Middle to Late Miocene.||||||01-SEP-08
23359|Bare Formation|41271|3|Fully described|p187|||||||||
23359|Bare Formation|41437|5|Briefly described|p76|||||||||
23359|Bare Formation|41438|6|Mentioned|p111|||||||||
23359|Bare Formation|41439|6|Mentioned|p124|||||||||
23359|Bare Formation|41732|6|Mentioned|Fig.3|||||||||
23359|Bare Formation|42116|6|Mentioned|p69|||||||||
23359|Bare Formation|43724|6|Mentioned|Fig.15,p65||Miocene|||||||
23359|Bare Formation|61155|5|Briefly described|p5, p15|Late Miocene|Late Miocene|Of the Cape Range Group. Mixed sandstone and dolomitic sequence. Max. thickness (offshore): 750m. Geological Province: Carnarvon Basin /offshore.||||||
23359|Bare Formation|62734|5|Briefly described|p1362 Fig. 2|Miocene|Miocene|Geological Province: Barrow Sub-basin.||||||01-SEP-08
23359|Bare Formation|62837|5|Briefly described|Stratigraphic columns|Middle Miocene|Middle Miocene|Age: ~15-~12Ma. Geological Province: Rankin Platform and Beagle Sub-basin.||||||01-MAR-10
23359|Bare Formation|67200|5|Briefly described|p8 fig 6, |Miocene|Oligocene|||||Overlies Trealla Limestone, overlain by Delambre Formation|Planar cross bedded sandstone.|
23359|Bare Formation|67368|6|Mentioned|p209 Fig.4.|Miocene|Miocene|||||Overlies Trealla Limestone.||
23359|Bare Formation|70066|5|Briefly described|Dampier: Fig.2. Exmouth: Fig.2|Miocene|Miocene|See also Regional: Fig.6. Northern Carnarvon Basin.||Cape Range Group.||Overlies Trealla Limestone. Is overlain by Delambre Formation.||
37722|Barimunya Member|24573|4|Described|p685, 688|||Of the Marillana Formation. Max Thickness: 70m. Geological Province: central Hamersley Range. Previously the upper part of the main "Main Pisolite Zone".||||||
37722|Barimunya Member|60539|5|Briefly described|p498, 500, 501 Fig.3, 517|Miocene|Miocene|Of the Marillana Formation. Geological Province: Pilbara Craton. Thickness: ~75 m. Overlies: Munjina Member. Underlies Iowa Eastern Member. Conglomerate, channel iron deposits, minor claystone, breccia and sandstone.||||||02-FEB-05
37722|Barimunya Member|63432|5|Briefly described|p734, p736 Fig. 3|||Of the Marillana Formation. Geological Province: Hamersley Province. Channel iron deposit.||||||07-FEB-11
37722|Barimunya Member|65194|5|Briefly described|p107, p111-112|||Unit in Marillana Formation; between Munjina and Iowa Eastern Members. Is the main channel iron deposit unit in the Formation, and consists of an unaltered upper, and groundwater-altered lower, sub-units.||||||
37722|Barimunya Member|69538|5|Briefly described|p522 Fig.5, p535, p557, p560 Fig.35|Miocene|Miocene|See also p572, p583-585. Billions of tonnes of channel iron deposits.||Unit in Marillana Formation.|||Pedogenic pelletoids and peloids; clay.|
37722|Barimunya Member|73574|5|Briefly described|p762|Miocene|Late Eocene|Central Hamersley region.||Marillana Formation||Overlies Munjina Member|Thick unit dominated by pisoids and pelletoids.|
23360|Barker Monzogranite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1860Ma. Geological province: Kimberley Province (West).||||||07-FEB-11
23360|Barker Monzogranite|42710|5|Briefly described|map legend|Proterozoic||||||||
23360|Barker Monzogranite|42811|5|Briefly described|p10|||||||||
23360|Barker Monzogranite|43281|5|Briefly described|Map legend||Proterozoic|||||||
23360|Barker Monzogranite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Paperbark Supersuite.||||||07-NOV-08
23360|Barker Monzogranite|70154|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic||1852-1862 Ma|Paperbark Supersuite|||Medium- to fine-grained biotite monzogranite; contains some small mafic inclusions.|
23360|Barker Monzogranite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 100k_geologyp_lut.csv.|1862-1852 Ma (inferred)|Unit of Paperbark Supersuite.|||Medium- to fine-grained biotite monzogranite; contains some small mafic inclusions|
23360|Barker Monzogranite|72437|5|Briefly described|p63|||Hooper Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Porphyritic monzogranite.|
70179|Barlangi Granophyre|61560|5|Briefly described|p494|||Interpreted to be an impact melt associated with the Yarrabubba impact structure.  Intrudes the Yarrabubba Granite. ||||||
70179|Barlangi Granophyre|61564|5|Briefly described|p593, p594 Fig. 7|||Pink brown, xencrysts and lithic fragments of granite - impact melt injected along a fault/fracture. Surrounded by shocked granitic rocks of Yarrabubba Granite displaying classic shatter cones and pseudotachylite veins. ||||||
70179|Barlangi Granophyre|64771|4|Described|p28-32|Neoarchaean|Neoarchaean|Centre of the Yarrabubba Impact Structure. Subcrater impact melt derived from Yarrabubba Granite: REE and trace element profiles are identical. Ar-Ar dating at 1134 Ma (Pirajno, 2005) may represent alteration age.|c.2.7-2.6 Ga.|||Hosted by Yarrabubba Granite.|Pink, fine-grained rock, with scattered coarser grains of quartz and feldspar, and xenoliths of coarse-grained granite that range from a few cms to 0.4 m across. Unusual skeletal textures. No quartz veins, mafic dykes, or pseudotachylites.|
70179|Barlangi Granophyre|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Proterozoic|Neoarchean|Yilgarn Craton. Sample 178063: All zircons analysed were xenocrystic therefore age is a maximum age for igneous crystallization of the host micromonzonite. |2793+/-4 Ma Pb/Pb SHRIMP||||Medium-grained, granophyric monzogranite; undeformed; local xenoliths of partly melted, coarse-grained granite|
70179|Barlangi Granophyre|69583|6|Mentioned|Plate 2||||||||Medium-grained, granophyric monzogranite.|
70179|Barlangi Granophyre|69628|5|Briefly described|map legend|Proterozoic|Proterozoic||||||Medium-grained, granophyric monzogranite; undeformed; local xenoliths of partly melted, coarse-grained granite.|
70179|Barlangi Granophyre|70796|5|Briefly described|100k_geologyp_lut.csv|Proterozoic|Neoarchean|Yilgarn Craton. See also 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 178063.1.pdf, Nowthanna100_2643_stratig.pdf.|ca 2800 to 541 Ma (inferred)||||Mediumgrained, granophyric monzogranite; undeformed; local xenoliths of partly melted, coarsegrained granite.|
70179|Barlangi Granophyre|70830|5|Briefly described|p15-p19|||||||||
70179|Barlangi Granophyre|71269|4|Described|GEOL_LUT_CSV files + geochron files|Proterozoic|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Yilgarn Craton events (4000-2600 Ma). Sample GSWA 178063 (micromonzonite) yielded a weighted mean 207Pb/206Pb age of 2647+\-11 Ma, interpreted to be maximum age for igneous crystallisation. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv.|2647-1210 Ma (inferred)||||Medium-grained, granophyric monzogranite; undeformed; local xenoliths of partly melted, coarse-grained granite.|
70179|Barlangi Granophyre|72034|5|Briefly described|500k_interpgeop16_lut|Proterozoic|Neoarchean||||||Medium-grained, granophyric monzogranite; undeformed; local xenoliths of partly melted, coarse-grained granite.|
74625|Barn Hill Formation|64449|4|Described|p75, p79 Tb. 5, p101-103|Holocene|Holocene|Overlies Mowanjum Sand, overlain by Church Hill Sand & Shoonta Hill Sand. Age: 2740+/-120 yrs BP and 900+/-100 yrs BP. Thick: 7m. Red quartz and quartz-and-carbonate sand. See p101-103.||||||07-FEB-11
74625|Barn Hill Formation|73213|5|Briefly described|958 Fig.3(a), 961 Fig.8, 967-968|||||||Overlies Mowanjum Sand.|A mixed facies of calcareous dunes and orange quartz sand dunes. Contains buried shell middens.|
82171|Barnicarndy Formation|73345|3|Fully described|p224, p226-227, p229-231|Paleozoic|Paleozoic|Newly defined. Canning Basin, Barnicarndy Graben. Has excellent potential for CO2 storage (with the Grant Group as a seal). Named after the Barnicarndy Hills. Type section is between 855 and 1345 m in Barnicarndy 1. Thickness of 490 m. Upper boundary is a major angular unconformity with the Grant Group. Boundaries represent very distinctive seismic reflectors. Potentially correlative to the Willara and Goldwyer formations or the Carribuddy Group. Includes bioturbation and tidal facies; indicates marine influence for at least part of the formation. Unit is separated into two distinct sandstone dominated intervals with a boundary at ca 1070 m in Barnicarndy 1 based on changes in paleo-flow directions and water salinity. [Misspelt as Barnicardy Formation on p226].||||Conformably underlain by Nambeet Formation (Samphire Marsh Member). Unconformably overlain by Grant Group.|Fine- to medium-grained oxidized quartz sandstones and minor siltstone.|
82171|Barnicarndy Formation|73346|6|Mentioned|p27, p30|Katian|Darriwilian|Canning Basin, Barnicarndy Graben. Thickness: c. 500 m. Age is a tentative maximum depositional age based on two analyses of the youngest detrital zircon.|456 +/- 8 Ma|||||
74901|Barracouta Shoal Formation|69297|6|Mentioned|p305|Holocene|Messinian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin. ||Woodbine Group||Overlies the Oliver Formation.||
74901|Barracouta Shoal Formation|69452|5|Briefly described|p36:15, 22|Holocene|Pliocene|Bonaparte Basin.||Woodbine Group.||||12-JUL-16
74901|Barracouta Shoal Formation|69673|6|Mentioned|p174|||||||||
74901|Barracouta Shoal Formation|70061|5|Briefly described|Regional geology Figs.6-7, p12|Holocene|Miocene|See also Sahul: Fig.2. Vulcan: Fig.2. [Misleadingly abbreviated to Barracouta Formation, a Victorian unit, on p12.]||Woodbine Group.||Overlies Oliver Formation.||12-JUL-16
74901|Barracouta Shoal Formation|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Holocene|Miocene|See also Northern: Fig.2. Yampi: Fig.2. Browse Basin.||Woodbine Group.||Overlies Oliver Formation.||12-JUL-16
74849|Barrambie Igneous Complex|44149|6|Mentioned|p120 Fig.2-125|||Appears as Barrambie Complex.||||||
74849|Barrambie Igneous Complex|64891|5|Briefly described|p37 Fig. 2, p42, p50-51 Tb. 1|Archean|Archean|Of the Meeline Suite. Age: c. 2780Ma. Geological province: Murchison Domain. Hosts vanadium mineralisation (mine is proposed). Layered gabbro and anorthosite, with magnetite and pyroxenite layers; metamorphosed.||||||07-FEB-11
74849|Barrambie Igneous Complex|66195|4|Described|p604, p598 Fig.1, p599 Fig.2, p602|Neoarchean||||In Meeline Suite.|||Main zone: gabbronorite and leucocratic magnetitite and leucogabbro and leucocratic gabbronorite (~1km thick). Upper zone: leucocratic magnetitite and leucogabbro and leucocratic anorthosite (~200m thick).|13-MAR-12
74849|Barrambie Igneous Complex|67129|5|Briefly described|p18 Fig.19, p51-52, p54, p60|Archean|Archean|Murchison Domain, Youanmi Terrane. Hosts significant vanadium mineralisation.||Meeline Suite.||||
74849|Barrambie Igneous Complex|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane||Meeline Suite|Includes 4 unnamed subunits.||Peridotitic schist; Peridotite; Anorthosite to gabbroic anorthosite; Layered gabbro, with minor pyroxenite, leucogabbro, and anorthosite; mostly metamorphosed|
74849|Barrambie Igneous Complex|69583|5|Briefly described|p49-50, p98, p102, p177; Plate 2|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Igneous stratigraphic column. The three Lithology facies are mapped separately.|||||Layered gabbro and anorthosite with magnetitite and pyroxenitic layers; magnetitite; peridotite; metamorphosed.|
74849|Barrambie Igneous Complex|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean|||Meeline Suite||||
74849|Barrambie Igneous Complex|69586|5|Briefly described|p22|Mesoarchean|Mesoarchean|Murchison Domain.||Meeline Suite.||||
74849|Barrambie Igneous Complex|69628|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Detailed lithology in legend. The five facies are mapped separately.||Meeline Suite|||Anorthosite to gabbroic anorthosite; magnetitite; layered gabbro, minor pyroxenite/leucogabbro/anorthosite; peridotitic schist, serpentine-chlorite-actinolite; peridotite, massive to weakly foliated (section only); metamorphosed.|
74849|Barrambie Igneous Complex|70419|5|Briefly described|p7-8|||Between 3 to 5 km thick; has distinctive magnetitite units in its upper zone.||Meeline Suite.||||
74849|Barrambie Igneous Complex|70420|5|Briefly described|p2, p4-5, p7-8, p10-11, p25-28, p31-32|||Southern Cross Domain, Youanmi Terrane, Yilgarn Craton. Features steep dips, poor outcrops and strong deformation within shear zones. The process of 3D modelling described; density and magnetic susceptibility values given.||Meeline Suite.||||
74849|Barrambie Igneous Complex|70796|5|Briefly described|100k_interpgeol_lut.csv,|Mesoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. See also 100K_interpgeop_lut.csv,  500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 194751.1.pdf, Nowthanna100_2643_stratig.pdf. Numerous additional lithologies are discussed.|ca 2815 Ma to 2800 Ma (inferred)||||Magnetite, peridotite, metamorphosed. Anorthosite, gabbroic anorthosite, layered gabbro, peridotitic schist.|
74849|Barrambie Igneous Complex|70830|5|Briefly described|p4, p19, p26-p27|||This unit is the type example for the Meeline Suite.||Meeline Suite|||Anorthosite, magnetite anorthosite, gabbro, magnetite gabbro and magnetite rocks.|
74849|Barrambie Igneous Complex|71311|6|Mentioned|p794|||Northern Youanmi Terrane, Yilgarn Craton.||||||
74849|Barrambie Igneous Complex|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Youanmi Terrane.||Meeline Suite|Includes unnamed member.||Layered gabbro and anorthosite with magnetitite and pyroxenitic layers; metamorphosed. Peridotite; fine to medium grained; massive to weakly foliated; metamorphosed.|
74273|Barrambie gabbro|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolerite, gabbro, pyroxenite, anorthosite|
74273|Barrambie gabbro|71269|6|Mentioned|1m_geologyp12_lut.csv||||||||Gabbro, pyroxenite, anorthosite, magnetite rock|
30675|Barramundi Conglomerate|24503|5|Briefly described|Map legend|Devonian|Devonian|Boulder, cobble and pebble conglomerate.  Geological Province: Canning Basin.||||||20-JUL-06
30675|Barramundi Conglomerate|43281|6|Mentioned|Map legend|Late Devonian|Late Devonian|Geol. Prov: Canning Basin.||||||20-JUL-06
30675|Barramundi Conglomerate|44231|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Boulder, cobble and pebble conglomerate; poorly exposed; interbedded locally with Nullara Limestone and ?Piker Hills Formation.  Age: Early to ?Middle Famennian. Geological Province: Canning Basin.||||||26-MAY-05
30675|Barramundi Conglomerate|64580|6|Mentioned|map legend|||Frasnian and Famennian conglomerates associated with Devonian reef complexes.||||||15-DEC-08
30675|Barramundi Conglomerate|66127|4|Described|pp139-142, pp144-145, Plates 3, 7. |Famennian|Late Devonian|Formerly the Burramundi Conglomerate of Guppy et al. (1958); renamed Barramundi Conglomerate by Griffin and Tyler (1995) and Tyler et al. (1998). Type locality is a deep gully on NE side of Barramundi Range. Deposited in front of the scarp of the Mount Elma (normal) Fault, active during the Famennian. Thickness c. 400 m.||||Interfingers with Nullara Limestone. Grades laterally into Piker Hills Formation.|Cobble to boulder conglomerate with minor intercalated coarse-grained sandstone and reefal carbonates; quartzite clasts dominant; alluvial-cone, fan-delta, and submarine-fan deposits.|
30675|Barramundi Conglomerate|69099|5|Briefly described|500k_geologyp08_lut.csv|Famennian|Frasnian|Frasnian and Famennian conglomerates associated with Devonian reef complexes|||||Conglomerate and sandstone.|30-JUL-15
30675|Barramundi Conglomerate|69165|6|Mentioned|500k_geologyp08_lut.csv|Famennian|Frasnian|||||||
30675|Barramundi Conglomerate|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Platform boulder, cobble and pebble conglomerate|
30675|Barramundi Conglomerate|71811|5|Briefly described|Map legend.|Famennian|Famennian|Canning Basin. A unit in the Devonian Reef Complexes: late Famennian platform and basin floor conglomerates associated with carbonate reef complexes.|||||Siliciclastic cobble to boulder conglomerate, minor sandstone.|06-MAY-19
32532|Barrar Member|64502|6|Mentioned|p785|||Of Napier Formation in Dingo Gap area.||||||10-NOV-08
32532|Barrar Member|66127|4|Described|p64, pp245-249, pp311-312, Plates 1,2.|Late Famennian|Middle Famennian|Named after the Aboriginal name for the valley at the SW entrance to the Tunnel Creek tunnel. 195 - 230 m thick.||Unit in Napier Formation.|||Fore-reef deposits: interbedded calcarenite alternating with debris-flow megabreccias; local enormous allochthonous blocks of reef limestone.|
29872|Bartle Member|7471|5|Briefly described|p8, Map legend|Proterozoic|Proterozoic|||Of Killara Formation.|||Complexly intermixed chert, cherty evaporitic units, and silicified pyroclastic material.|
29872|Bartle Member|12099|5|Briefly described|p678 Fig.4, p679|Paleoproterozoic|Paleoproterozoic|New or redefined unit by Occhipinti et al. (1997). Represents the final quiescent stage of Killara volcanic activity in an environment of salt lakes and localised hot springs.||Unit in Killara Formation.|||Volcaniclastic, evaporitic and chemical sedimentary rocks.|04-MAR-13
29872|Bartle Member|22899|5|Briefly described|85|||Geol province Yerrida Basin. Parent Killara Formation||||||
29872|Bartle Member|23581|5|Briefly described|Map legend||Paleoproterozoic|Of the Killara Formation in the Mooloogool Subgroup in the Yerrida Group in the Yerrida Basin.||||||24-JUN-09
29872|Bartle Member|23589|5|Briefly described|p18|||Of Killara Formation.||||||
29872|Bartle Member|23593|5|Briefly described|p11|||Of Killara Formation. Geological Province: Yerrida Basin.||||||
29872|Bartle Member|23600|4|Described|p12|||Of Killara Formation. Geological Province: Yerrida Basin.||||||
29872|Bartle Member|23611|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|See also page 33 Appendix 1. Of Killara Formation. Geological Province: Yerrida Basin.||||||07-NOV-08
29872|Bartle Member|23865|3|Fully described|p172|Paleoproterozoic|Paleoproterozoic|Of Killara Formation, Mooloogool Subgroup. Geological Province: Yerrida Basin. Maximum thickness:~30m.||||||07-NOV-08
29872|Bartle Member|43836|5|Briefly described|Map Legend||Proterozoic|||||||
29872|Bartle Member|43837|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Killara Formation.  Laminated chert.||||||18-MAY-04
29872|Bartle Member|49893|4|Described|p15|Proterozoic|Proterozoic|Of the Killara Formation (Yerrida Group). Geological Province: Yerrida Basin. Max. Thickness: ~10m. Contains some rocks previously included in the Maraloou Formation and Narracoota Formation. See also p6 Fig.3.||||||24-JAN-06
29872|Bartle Member|49912|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Killara Formation (Yerrida Group).  Chertified microbial laminites with barite and anhydrite nodules.  Geological Province: Yerrida Basin.||||||
29872|Bartle Member|50222|5|Briefly described|p320 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Killara Formation (Moogoolool Group).  Geological Province: Yerrida Basin.||||||07-NOV-08
29872|Bartle Member|62289|4|Described|plate 1, p7 Fig. 3, p16, p19-21|Palaeoproterozoic|Palaeoproterozoic|Top of Killara Formation, Mooloogool Subgroup (Yerrida Group), represents end-phase of volcanic activity; type area is NW and E of White Well; chertified microbial laminite, chert breccia, and chemical sedimentary, and chertified volcaniclastic rocks.||||||
29872|Bartle Member|62353|5|Briefly described|map legend|Proterozoic|Proterozoic|Geol. Prov: Yerrida Basin.||Of Killara Formation (Mooloogoo Subgroup, Yerrida Group).|||Chert, chert breccia, laminated chert, and chertified sedimentary rock; locally with pseudomorphs of anhydrite crystals and nodules; minor basaltic lava.|14-APR-11
29872|Bartle Member|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Of Killara Formation. Chertified microbial laminite; chert breccia; chemical sedimentary; and chertified volcaniclastic rock; pseudomorphs of barite and anhydrite nodules.||||||15-DEC-08
29872|Bartle Member|65264|5|Briefly described|p27, p44 Appdx. 1|||Of the Killara Formation (Mooloogool Sugroup). Geological province: Yerrida Basin. Comprises variably laminated or brecciated chert and chertified sedimentary rocks with evaporitie affinities.||||||07-FEB-11
29872|Bartle Member|65419|2|Defined|pp19-20, pp22-23.|Paleoproterozoic|Paleoproterozoic|Named after Mount Bartle. No type section; type area lies immediately to NW, extending to the east, of White Well. A lenticular unit 5 m (to 30 m) thick. Lies in close association with, and at the top of, the Killara Formation. Probable sodic lacustrine setting at closing phases of volcanism. Included as 'chert, chert breccia' in the Maraloou Formation by Elias et al. (1982); later as 'cherty interflow sediments' of the Narracoota Volcanics by Gee and Grey (1993).||Unit in Killara Formation.||Interfingers with overlying Maraloou Formation.|Chert, associated chertified evaporitic units, chert breccia, silicified fine pyroclastic material; complexly intermixed; white plate-like quartz and evaporite minerals (anhydrite, gypsum, possibly shortite) occur.|
29872|Bartle Member|65472|6|Mentioned|p3 Fig.2|||Yerrida Basin.||||||
29872|Bartle Member|65913|3|Fully described|p3 Table 1, pp11-14. |Paleoproterozoic|Paleoproterozoic|A variety of shallow-water or subaerial sedimentary rocks including chemical sediments (possibly hot-spring deposits) and evaporites. The chert and chert breccia were formerly mapped as part of Maraloou Formation (Elias et al. 1982); defined as part of Narracoota Volcanics (Gee and Grey 1993). Geochemical analysis is detailed. Contains anomalous Au values of 35 - 66 ppb.||Unit in Killara Formation.||Is overlain by Maraloou Formation.|Massive and laminated cherts, chert breccia, chertified sedimentary rocks and welded pyroclastics; septarian nodular concretions; chalcedonic cement; plate-like quartz with surficial moulds, possibly evaporite replacement or sinter-like precipitate.|
29872|Bartle Member|69003|5|Briefly described|p12|||Yerrida Basin.||Killara Formation.||Is overlain conformably by Bubble Well Member.|Evaporites.|
29872|Bartle Member|69152|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin||Killara Formation|||Chert, chert breccia, laminated chert, and silicified sedimentary rock; locally with pseudomorphs of anhydrite crystals and nodules; minor volcaniclastic rocks.|05-AUG-15
29872|Bartle Member|70153|5|Briefly described|100k_geologyp10_lut.csv|Paleoproterozoic|Paleoproterozoic||1652 Ma (inferred).|Killara Formation|||Chert, chert breccia, laminated chert, and silicified sedimentary rock; locally with pseudomorphs of anhydrite crystals and nodules; minor volcaniclastic rocks.|
29872|Bartle Member|70804|5|Briefly described|p2|||New name.||Killarra Formation||||
29872|Bartle Member|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||chert, siltstone, ironstone, ash tuff|
29872|Bartle Member|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen. Of Earaheedy Basin. See 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.||Unit of Killara Formation.|||Chert, chert breccia, laminated chert, and silicified sedimentary rock; locally with pseudomorphs of anhydrite crystals and nodules; minor volcaniclastic rocks|
38798|Barton Dolerite|23926|6|Mentioned|p33 Fig. 15|||Geological Province: Yilgarn Craton.||||||
38798|Barton Dolerite|23931|6|Mentioned|p200 Fig.2|||Geological Province: Yilgarn Craton.||||||
38798|Barton Dolerite|60979|5|Briefly described|p92, p86 Fig.2, p90|||Part of the Jundee sequence - Jundee goldfield area. See also p91 Fig.4. Thickness: ~100-190m. Fine- to coarse-grained ophitic to sub-ophitic dolerite and quartz granophyre overlying clinopyroxene cumulate.||||||
75923|Baseline Orthogneiss|66113|5|Briefly described|Map legend|Archean|Archean|Burtville Terrane, Yilgarn Craton. Unit in Minigwal Suite. Migmatitic orthogneiss.||||||
75923|Baseline Orthogneiss|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Burtville Terrane, Eastern Goldfields Superterrane, Yilgarn Craton||Minigwal Suite|||Migmatitic orthogneiss.|05-AUG-15
75923|Baseline Orthogneiss|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|See also 100k_geologyp14_lut.csv and 500k_interpgeop14_lut.csv.|2769 - 2765 Ma (inferred).|Minigwal Suite|||Migmatitic orthogneiss.|
75923|Baseline Orthogneiss|70802|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Burtville Terrane, Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events.|2769-2765 Ma (inferred)|Unit of Minigwal Suite.|||Migmatitic orthogneiss|
75923|Baseline Orthogneiss|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Burtville Terrane, Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 100k_geologyp14_lut.csv, 500k_interpgeop_lut.csv.|2769-2765 Ma (inferred)|Unit of Minigwal Suite.|||Migmatitic orthogneiss|
75923|Baseline Orthogneiss|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|||Minigwal Suite|||Migmatitic orthogneiss.|
25776|Bassendean Sand|12759|4|Described|p47-9; p28 Tb. 7; p32 Fig 15; P36 Fig 17|Quaternary||Defined Playford and Low (1972). Type area in Bassendean suburb, Perth. Max thickness - 80 m.||||Conformable on Gnangara Sand. Interfingers with Guildford Clay. Overlain unconformably by Tamala Limestone.|Sand; grey-brown to whitish-grey, fine to coarse, poorly sorted, weakly iron-oxide cemented ("coffee rock") near base, common black heavy minerals throughout but locally concentrated.|12-MAY-14
25776|Bassendean Sand|22552|6|Mentioned|p 35, 37|||||||||
25776|Bassendean Sand|22820|6|Mentioned|p23|Quaternary|Quaternary|Part of the Quaternary deposits unconformably overlying the Cretaceous rocks of the southern Perth Basin, including Warbro Group units.||||||12-AUG-08
25776|Bassendean Sand|23768|5|Briefly described|p30 Fig.6|Pleistocene|Pleistocene|Geological Province: Perth Basin.||||||30-MAR-05
25776|Bassendean Sand|24094|6|Mentioned|p275|||Geological Province: Perth Basin||||||16-MAR-05
25776|Bassendean Sand|24160|6|Mentioned|p88-90, p94|Quaternary|Quaternary|Perth Basin.|||||Sandy colluvium.|
25776|Bassendean Sand|24410|4|Described|p40|Pleistocene|Pleistocene|Of Kwinana Group. Clean, well rounded and sorted; high iron, yellow to brown, some hard ferruginous material. Overlies the Guildford Formation. Geological Province: Perth Basin.||||||24-NOV-09
25776|Bassendean Sand|24464|5|Briefly described|p331|||Underlain by Ascot Formation.||||||
25776|Bassendean Sand|29382|6|Mentioned|Fig.13|||||||||
25776|Bassendean Sand|29383|6|Mentioned|Table 3|||||||||
25776|Bassendean Sand|29693|6|Mentioned|Fig.6|||||||||
25776|Bassendean Sand|30217|6|Mentioned|p21|||Sand dune systems||||||
25776|Bassendean Sand|30939|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
25776|Bassendean Sand|30963|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
25776|Bassendean Sand|30966|6|Mentioned|p27|||See also P28. Possible source of water||||||
25776|Bassendean Sand|31027|6|Mentioned|p56|||||||||
25776|Bassendean Sand|31896|6|Mentioned|p33|||||||||
25776|Bassendean Sand|31910|4|Described|Table 1|||||||||
25776|Bassendean Sand|32650|2|Defined|p90|late Pleistocene|middle Pleistocene|Probably Middle to Late Pleistocene.||||||
25776|Bassendean Sand|33044|4|Described|p58|||See also diagrams 17 and 18; and maps 3 and 4||||||07-AUG-07
25776|Bassendean Sand|33747|5|Briefly described|p1071|||||||||
25776|Bassendean Sand|35041|6|Mentioned|p367|||||||||
25776|Bassendean Sand|35056|6|Mentioned|p90|||||||||
25776|Bassendean Sand|35638|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
25776|Bassendean Sand|35968|6|Mentioned|Fig.8|||||||||
25776|Bassendean Sand|36293|3|Fully described|p209|||||||||
25776|Bassendean Sand|36890|5|Briefly described|p255|||||||||
25776|Bassendean Sand|37001|6|Mentioned|p28|||||||||
25776|Bassendean Sand|37017|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
25776|Bassendean Sand|37309|5|Briefly described|p16|||||||||
25776|Bassendean Sand|37577|6|Mentioned|p80|||||||||
25776|Bassendean Sand|38479|4|Described|p19|||||||||
25776|Bassendean Sand|38777|4|Described|p30|||||||||
25776|Bassendean Sand|38807|6|Mentioned|p10|||||||||
25776|Bassendean Sand|38997|4|Described|p5|||||||||
25776|Bassendean Sand|39554|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
25776|Bassendean Sand|39829|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
25776|Bassendean Sand|39915|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
25776|Bassendean Sand|40304|5|Briefly described|p42|||||||||
25776|Bassendean Sand|40348|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
25776|Bassendean Sand|40349|6|Mentioned|Table 2|||||||||
25776|Bassendean Sand|40359|5|Briefly described|p28|||||||||
25776|Bassendean Sand|40360|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
25776|Bassendean Sand|40367|6|Mentioned|Table 1 p72|||Of Seddon (1972), Playford et al (1976). Part of the Bassendean Dune System.||||||07-AUG-07
25776|Bassendean Sand|40401|6|Mentioned|p122|||||||||
25776|Bassendean Sand|40902|6|Mentioned|p55|||||||||
25776|Bassendean Sand|40991|5|Briefly described|p6|||||||||
25776|Bassendean Sand|41251|4|Described|p36|||||||||
25776|Bassendean Sand|41344|6|Mentioned|p172|||||||||
25776|Bassendean Sand|41346|6|Mentioned|p26|||||||||
25776|Bassendean Sand|41504|6|Mentioned|p71|||||||||
25776|Bassendean Sand|41634|4|Described|p41|||||||||
25776|Bassendean Sand|41782|4|Described|p24|||||||||
25776|Bassendean Sand|41783|4|Described|p48|||||||||
25776|Bassendean Sand|41788|5|Briefly described|p109|||||||||
25776|Bassendean Sand|41789|5|Briefly described|p87|||||||||
25776|Bassendean Sand|41986|4|Described|p40|||||||||
25776|Bassendean Sand|42009|6|Mentioned|p75|||||||||
25776|Bassendean Sand|42687|6|Mentioned|map legend|||||||||
25776|Bassendean Sand|42688|6|Mentioned|map legend|||||||||
25776|Bassendean Sand|43062|4|Described|p27,table 2.p18|||||||||
25776|Bassendean Sand|43066|5|Briefly described|Fig.2,p102|||||||||
25776|Bassendean Sand|43096|5|Briefly described|p6|||||||||
25776|Bassendean Sand|43189|5|Briefly described|Map Legend||Quaternary|||||||
25776|Bassendean Sand|43197|5|Briefly described|Map Legend||Quaternary|||||||
25776|Bassendean Sand|43212|5|Briefly described|p6||Pleistocene|||||||
25776|Bassendean Sand|43231|5|Briefly described|p4|||||||||
25776|Bassendean Sand|43304|5|Briefly described|Map Legend||Pleistocene|||||||
25776|Bassendean Sand|43306|5|Briefly described|Map Legend||Quaternary|||||||
25776|Bassendean Sand|43308|5|Briefly described|Map Legend||Quaternary|||||||
25776|Bassendean Sand|43309|5|Briefly described|Map Legend||Quaternary|||||||
25776|Bassendean Sand|43347|4|Described|10|||prev. Guildford FM.||||||
25776|Bassendean Sand|44144|4|Described|p501 Tb.4-21, p520 Fig.4-165|Pleistocene|Pleistocene|Type area: Bassendean (no type section selected). 45m thick forming Bassendean Dune System.||Kwinana Group|||Quartz sand.|
25776|Bassendean Sand|63330|5|Briefly described|p192|Pleistocene|Pleistocene|Underlies the Bassendean Dunes. Quartz sand. Geological Province: Perth Basin/Swan Coastal Plain.||||||31-JAN-08
25776|Bassendean Sand|63745|5|Briefly described|p59, p63|||Overlies Guildford Formation. Sandy fluvial and estuarine sediments. Locally contains pods and lenses of more clayey material.||||||07-FEB-11
25776|Bassendean Sand|67135|6|Mentioned|p64, p65 Fig.88.|||Source of high-silica sand for glass manufacture, filtering and blasting, and export.||||||
25776|Bassendean Sand|68811|5|Briefly described|p90, p94|Quaternary|Neogene|One of a group of 'superficial sediments' described as being up to 90m thick.|||||Group description: Sand, limestone, silt and clay.|15-APR-20
25776|Bassendean Sand|69081|6|Mentioned|p737 Fig.1|||Geol. Prov: Perth Basin||||||
25776|Bassendean Sand|69558|6|Mentioned|p103|||Formed by dissolution of the Tamala Limestone. ||||||
25776|Bassendean Sand|69788|6|Mentioned|p1025|Pleistocene|Pleistocene|Swan Coastal Plain. Also known as Bassendean Dune System.|||||Siliceous.|
25776|Bassendean Sand|69840|6|Mentioned|p183|Pleistocene|Neogene|Alternate name for Bassendean Dune System.||||||
25776|Bassendean Sand|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||coastal sediment, aeolian sand|
25776|Bassendean Sand|71958|5|Briefly described|p35|Holocene|Holocene|Vlaming Sub-basin. Of the Bassandean Dune System.||||||
79851|Bassetts Volcanic Member|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.|2800-2760 Ma|Unit of Meekatharra Formation.|||Pyroxene spinifex-textured basalt with boninitic affinity; metamorphosed and locally schistose|
79851|Bassetts Volcanic Member|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.||Meekatharra Formation.|||Pyroxene spinifex-textured basalt with boninitic affinity; metamorphosed and locally schistose.|
79851|Bassetts Volcanic Member|72389|5|Briefly described|Map Legend|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Gabanintha 1:100k map sheet 2644.||Meekatharra Formation|||Pyroxene spinifex-textured basalt with bonininitic affinity; metamorphosed and locally schistose.|28-AUG-20
74827|Batchelor Monzogranite|64891|5|Briefly described|p37 Fig. 2, p38, p50-51 Tb. 1|Archean|Archean|Of Big Bell Suite (Austin Downs Supersuite). Age: ?2710Ma. Geological province: Murchison Domain. Monzogranite, commonly foliated; metamorphosed.||||||07-FEB-11
78610|Bayleys Monzogranite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Age inferred.|2726 - 2692 Ma.||||Fine-grained microgranite; quartz and feldspar phenocrysts; metamorphosed.|
78610|Bayleys Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2726-2692 Ma (inferred)||||Fine-grained microgranite; quartz and feldspar phenocrysts; metamorphosed|
40750|Beabea Monzogranite|24554|4|Described|p5 Tb.1, p8|Archean|Archean|Of the Yule Granitoid Complex. Age: 2945 +/- 4 Ma (U-Pb. Nelson, 2002). Geological Province: East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
40750|Beabea Monzogranite|50146|5|Briefly described|Map Legend|Archean|Archean|Of the Yule Granitoid Complex. Age: c. 2941 Ma. Geological Province: Pilbara Craton. Equigranular to feldspar porphyritic biotite monzogranite; weakly to moderately foliated.||||||07-NOV-08
40750|Beabea Monzogranite|63441|5|Briefly described|p10 Tb. 2|Archean|Archean|Of Sisters Supersuite. Age: 2941+/-5 Ma. Geological province: Pilbara Craton.||||||15-APR-13
40750|Beabea Monzogranite|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Unit in Sisters Supersuite. c. 2941 Ma. Biotite monzogranite; equigranular to feldspar-porphyritic; weakly to moderately foliated.||||||15-APR-13
40750|Beabea Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|Age derived from sample of seriate biotite monzogranite (169018.1.pdf)|2941 Ma +/- 5 Ma (SHRIMP)|Sisters Supersuite|||Biotite monzogranite; equigranular to feldspar-porphyritic; weakly to moderately foliated.|
40750|Beabea Monzogranite|69590|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; North Pilbara Orogeny. Sample GSWA 169018 (biotite monzogranite) yielded an interpreted igneous crystallisation age of 2941+\-5 Ma for the monzogranite (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|2941 Ma (isotopic)|Unit of Sisters Supersuite.|||Biotite monzogranite; equigranular to feldspar-porphyritic; weakly to moderately foliated|
40750|Beabea Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
40750|Beabea Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||2941+/-4 Ma|Sisters Supersuite|||Biotite monzogranite; equigranular to feldspar porphyritic; weakly to moderately foliated.|
23368|Beagle Bay Member|40837|6|Mentioned|p264|||||||||
23368|Beagle Bay Member|41215|6|Mentioned|p262|||||||||
31774|Bearra Gneiss|23569|4|Described|p6 Tb. 1|Archean|Archean|Of the Murchison Granite-Greenstone Terrane.   Dioritic and leucogranitic gneiss, possibly an earlier phase of the Tching Granite.||||||07-NOV-08
31774|Bearra Gneiss|23574|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Tching Granite.||||||07-NOV-08
31774|Bearra Gneiss|23576|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Tching Granite.||||||07-NOV-08
31774|Bearra Gneiss|23577|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Tching Granite.||||||07-NOV-08
31774|Bearra Gneiss|24114|5|Briefly described|p5 Fig.4|Archean|Archean|Geological Province: Yilgarn Craton. Age: c. 3280 Ma & 2720-2690 Ma.||||||07-NOV-08
31774|Bearra Gneiss|43835|5|Briefly described|Map Legend|Archean|Archean|||||||07-NOV-08
31774|Bearra Gneiss|71269|5|Briefly described|1m_geologyp12_lut.csv|||Containing zircon xenocrysts with ages of c. 4000 Ma, 3982 Ma, and 3945 Ma.|||||Dioritic gneiss (c. 3280 Ma) and leucocratic gneiss (c. 2720 Ma - igneous mafic intrusive).|
31774|Bearra Gneiss|73526|6|Mentioned|p2 Fig.1|||||||||
23370|Bearuroo Dolomite Member|24183|6|Mentioned|p12|||Correlated to the Cheyne Springs Formation.||||||
23370|Bearuroo Dolomite Member|40088|6|Mentioned|p227|||||||||
23370|Bearuroo Dolomite Member|40089|2|Defined|p41|Mesoproterozoic|Mesoproterozoic|||||||
25778|Beasley River Quartzite|22484|5|Briefly described|p77 Fig.6|||||||||
25778|Beasley River Quartzite|23047|5|Briefly described|40|||Of the Wyloo Group. Hamersley Province.  Max thickness 400 m. Overlain by Cheela Springs Basalt.||||||10-FEB-09
25778|Beasley River Quartzite|23280|5|Briefly described|p1085-6,Fig2p1086|||||||||
25778|Beasley River Quartzite|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Wyloo Group.||||||
25778|Beasley River Quartzite|23575|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Wyloo Group. Overlying unit Cheela Springs Basalt.||||||
25778|Beasley River Quartzite|23612|5|Briefly described|p841|Proterozoic|Archean|Of Wyloo Group. Geological Province: Hamersley Basin. Max. thickness: 500 m.||||||07-NOV-08
25778|Beasley River Quartzite|23774|5|Briefly described|p733 table 1||Paleoproterozoic|Minimum Age: 2209+/-15 Ma from overlying unit. Of Wyloo Group.||||||17-NOV-10
25778|Beasley River Quartzite|24544|4|Described|p47 Fig.35|Paleoproterozoic|Paleoproterozoic|Basal unit of Lower Wyloo Group. Unconformably overlies Kazput Formation, and many other formations of Mount Bruce Supergroup. Conformably overlain by Cheela Springs Basalt. Thickness: 220-360 m. Shallow marine. Geological Province: Ashburton Province.||||||07-NOV-08
25778|Beasley River Quartzite|24602|5|Briefly described|p854 Fig. 1|||Also referred to as BRQ in figure. Of the Wyloo Group.||||||
25778|Beasley River Quartzite|24607|4|Described|p967|Paleoproterozoic|Paleoproterozoic|Basal unit of the Wyloo Group. Overlain by the Cheela Springs Basalt. Shallow marine. Contains detrital zircons giving a maximum depositional age of 2446 +/- 8 Ma. Geological Province: Ashburton Basin.||||||30-NOV-10
25778|Beasley River Quartzite|29716|4|Described|Table 1|||||||||
25778|Beasley River Quartzite|33543|6|Mentioned|p132|||Refers de la Hunty (1965)||||||
25778|Beasley River Quartzite|33544|6|Mentioned|p34|||||||||
25778|Beasley River Quartzite|34066|4|Described|p7|||L.Prot.||||||
25778|Beasley River Quartzite|35218|6|Mentioned|Fig.1|||||||||
25778|Beasley River Quartzite|35260|5|Briefly described|p17|||||||||
25778|Beasley River Quartzite|35976|2|Defined|p108|Proterozoic|Proterozoic|||||||
25778|Beasley River Quartzite|36551|6|Mentioned|Table 23|||||||||
25778|Beasley River Quartzite|36882|4|Described|p136|||||||||
25778|Beasley River Quartzite|36883|6|Mentioned|p144|||||||||
25778|Beasley River Quartzite|36891|5|Briefly described|p441|||||||||
25778|Beasley River Quartzite|36902|6|Mentioned|p15|||||||||
25778|Beasley River Quartzite|37327|6|Mentioned|p393|||||||||
25778|Beasley River Quartzite|37460|3|Fully described|p121|||||||||
25778|Beasley River Quartzite|38321|6|Mentioned|Table 1|||||||||
25778|Beasley River Quartzite|38482|6|Mentioned|p15|||See also Table 4.||||||
25778|Beasley River Quartzite|39210|5|Briefly described|Table 1|||||||||
25778|Beasley River Quartzite|40103|6|Mentioned|Fig.1|||||||||
25778|Beasley River Quartzite|40369|6|Mentioned|Plate 1|||||||||
25778|Beasley River Quartzite|40905|5|Briefly described|p70|||||||||
25778|Beasley River Quartzite|40937|6|Mentioned|p28|||||||||
25778|Beasley River Quartzite|41243|6|Mentioned|p258|||||||||
25778|Beasley River Quartzite|41845|6|Mentioned|Fig. 1|||||||||
25778|Beasley River Quartzite|41955|6|Mentioned|Fig.1 P4|||||||||
25778|Beasley River Quartzite|42013|5|Briefly described|Map Legend|Proterozoic||||||||
25778|Beasley River Quartzite|42148|6|Mentioned|p687|||||||||
25778|Beasley River Quartzite|42260|3|Fully described|p11|||||||||
25778|Beasley River Quartzite|42277|6|Mentioned|p55|||||||||
25778|Beasley River Quartzite|42435|5|Briefly described|p46|||||||||
25778|Beasley River Quartzite|42471|4|Described|p10|||||||||
25778|Beasley River Quartzite|42472|5|Briefly described|Map legend|||||||||
25778|Beasley River Quartzite|42686|5|Briefly described|map legend|Proterozoic||||||||
25778|Beasley River Quartzite|42704|5|Briefly described|Plate 2E|Proterozoic||Basal unit of the Wyloo Group. Fine to coarse sandstone, may be silicified.  Intruded by dolerite sills.||||||07-AUG-08
25778|Beasley River Quartzite|42744|4|Described|p6|||||||||
25778|Beasley River Quartzite|42898|5|Briefly described|Fig.2 P341|||of Wyloo Group||||||
25778|Beasley River Quartzite|43037|5|Briefly described|Fig.2,p24|||of Wyloo Group||||||
25778|Beasley River Quartzite|43119|5|Briefly described|p13|||of Wyloo Group||||||
25778|Beasley River Quartzite|43262|5|Briefly described|Map Legend||Proterozoic|of Wyloo Group||||||
25778|Beasley River Quartzite|43290|4|Described|p8||Proterozoic|of Wyloo Group.||||||
25778|Beasley River Quartzite|43595|5|Briefly described|Table 3-8,p344||Paleoproterozoic|||||||07-NOV-08
25778|Beasley River Quartzite|44141|6|Mentioned|p307, p308|||Part source for Bresnahan Group conglomerates.||||||
25778|Beasley River Quartzite|44152|6|Mentioned|p188 Fig.2-161, p189|||||Basal Wyloo Group.|Three Corner Conglomerate Member.|Overlies Turee Creek Group. Is overlain by Cheela Springs Basalt.||
25778|Beasley River Quartzite|44477|14|Not recorded|p.11, Table 1||Proterozoic|SF/50-6.||||||
25778|Beasley River Quartzite|44478|14|Not recorded|map legend||Proterozoic|||||||
25778|Beasley River Quartzite|44481|5|Briefly described|map legend||Paleoproterozoic|||||||07-NOV-08
25778|Beasley River Quartzite|44692|2|Defined|p.7,17-19,Tb.1, map|||(F50-11),||||||
25778|Beasley River Quartzite|44729|5|Briefly described|map legend|Proterozoic||Of Wyloo Group||||||
25778|Beasley River Quartzite|50226|5|Briefly described|p415|Paleoproterozoic|Paleoproterozoic|Of the Wyloo Group.||||||07-NOV-08
25778|Beasley River Quartzite|61276|4|Described|p578|Orosirian|Orosirian|Lowermost unit in the Wyloo Group. Fluvial to shallow marine sediments. Outcrops of othoquartzites intruded by mafic sills were previously assigned to this unit in the Turee Creek Syncline, but are now believed to belong to Turee Creek Group. Unconformably overlies Turee Creek Group (~370 million year hiatus).||||Overlain by Cheela Springs Basalt.  Unconformably overlies Turee Creek Group (~370 million year hiatus).||17-OCT-16
25778|Beasley River Quartzite|61526|5|Briefly described|p879, p882|||Of the Lower Wyloo Group. Unconformably overlies parts of Turee Creek Group; unconformably overlain by Cheela Springs Group. See also p883.||||||
25778|Beasley River Quartzite|62129|3|Fully described|p11, p14, p19, p22|Archaean|Archaean|Of Wyloo Group. Uncomformably underlain by Kazput Formation. Thickness: 250m. Geological Province: Ashburton Basin. Cream- or white-weathering fine- to coarse-grained quartz sandstone, intruded locally by dolerite sills. Jaspilitic BIF-derived conglomerate at base. See p 14 for more detailed info.||||||15-DEC-22
25778|Beasley River Quartzite|62130|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Wyloo Group. Geological Province: Ashburton Basin. Fine- to coarse-grained metamorphosed quartzitic sandstone, metamorphosed ferruginous sandstone and conglomerate, and pelite; intruded by metadolerite sills.||||||
25778|Beasley River Quartzite|63866|5|Briefly described|p154|||||Mount Bruce Supergroup||Overlain by the Cheela Springs Basalt.||
25778|Beasley River Quartzite|63869|5|Briefly described|p5|Paleoproterozoic|Paleoproterozoic|SHRIMP U-Pb maximum age from detrital zircons.|<2446 +/- 8 Ma (GSWA, 2005).|Basal unit in Wyloo Group.||||
25778|Beasley River Quartzite|64384|5|Briefly described|p46, p47 Tb. 7|||Lower unit of Wyloo Group. Geological province: Ashburton Basin. Comprises silicified quartz sandstone + locally dev'd BIF-derived conglomerate, mudstone, + carbonate as part of a fan-delta system. Unconformable on Woongarra Volcanics, in E. See also p63||||||07-FEB-11
25778|Beasley River Quartzite|64580|6|Mentioned|map legend|||Of Wyloo Group, Lower.||||||15-DEC-08
25778|Beasley River Quartzite|64728|6|Mentioned|p107.|||Contains detrital zircons with ages from c.3550 Ma to 2450 Ma.||Unit in lower Wyloo Group.||||
25778|Beasley River Quartzite|65830|6|Mentioned|p3|||||Of the Wyloo Group||Overlain by the Cheela Springs Basalt.||
25778|Beasley River Quartzite|66115|5|Briefly described|p137 Fig.1|Paleoproterozoic|Paleoproterozoic|||Wyloo Group||||
25778|Beasley River Quartzite|66359|5|Briefly described|e96|||Intruded by undated dolerite sills at eastern end of Hardey syncline, Wyloo Dome and Duck Creek syncline. Overlain by Cheela Springs Basalt. Youngest detrital zircon in this unit (BRQ) is 2420 +/-18 Ma (GSWA 2005), but younger potential source rocks (dolerite dykes) contain no zircon.||||||
25778|Beasley River Quartzite|66574|5|Briefly described|p914 Fig.3, p916 Fig.4, p917 Fig.5|||Part of the lower Wyloo Group. Includes Three Corner Conglomerate Member. Underlies Nummana Member, overlies Kazput Formation. Fluvial to shallow marine conglomerate, sandstone; dolerite sills.||||||
25778|Beasley River Quartzite|66950|5|Briefly described|p4|Rhyacian|Rhyacian|||Of the Wyloo Group.||Overlain by the Cheela Springs Basalt.||
25778|Beasley River Quartzite|67025|6|Mentioned|p319.|Paleoproterozoic|Paleoproterozoic|||Basal unit in Wyloo Group.||||
25778|Beasley River Quartzite|67056|5|Briefly described|p419 Fig.2, pp440-441.|Paleoproterozoic|Paleoproterozoic|Includes a basal BIF-rich conglomerate.||Unit in Lower Wyloo Group.||Is overlain by Cheela Springs Basalt.||
25778|Beasley River Quartzite|67130|5|Briefly described|p3 fig 2, p4, p6, p10, p24 fig 17, p39||Rhyacian|Maximum of 360m thick. Age is maximum age of deposition. Misspelt as Beazly River Quartzite (p39 fig 36)|c. 2210 Ma|Wyloo Group, Lower|Includes Three Corners Conglomerate Member, Nummana Member|Conformably overlain by Cheela Springs Basalt, Nummana Member, unconformably overlies Turee Creek Group|Quartzite, quartz rich sandstone with local, well developed cross bedding.|
25778|Beasley River Quartzite|67829|6|Mentioned|p451.|||Occurs at the base of the lower Wyloo Group.||Unit in Wyloo Group.||||
25778|Beasley River Quartzite|67843|5|Briefly described|p33.|||Ashburton Basin. Detrital zircons suggest a similar source as the underlying Hamersley and Turee Creek Groups.||Unit in Wyloo Group.||||
25778|Beasley River Quartzite|67855|4|Described|p210-214, fig 3-10, p223, 225, 228|Paleoproterozoic|Paleoproterozoic|Mostly 220 - 360 m thick.||Of Wyloo Group (lowest part of).||Overlies Woongarra Volcanics or Weeli Wolli Formation.  Overlies Hamersley Group (unconformably).|Cream or white-weathering  silicified quartz sandstone with locally developed BIF-derived conglomerate, mudstone, carbonate.|
25778|Beasley River Quartzite|68035|4|Described|p293, p292 fig 6|Paleoproterozoic|Paleoproterozoic|Ashburton Basin. Up to 360 m thick. Cut by dolerite dykes emplaced at 2.01 Ga.|[<]2421+/- 25 Ma det[rital zircon?]|Of lower Wyloo Group.|Appears to include Three Corner Conglomerate Member, Nummana Member.|Unconformably overlies Kazput Formation, Turee Creek Group.  Conformably overlain by Cheela Springs Basalt, Wooly Dolomite.|Quartzite, sandstone, siltstone, conglomerate|23-DEC-15
25778|Beasley River Quartzite|68280|5|Briefly described|p5, p44, p51, p54, p62|Paleoproterozoic|Paleoproterozoic|Incorrectly spelled Beazly River Quartzite (p62 fig 67)|>2421 +/- 25 Ma|Wyloo Group, lower||Overlain by Nummana Member, overlies Three Corners Conglomerate Member unconformably overlies Turee Creek Group|Cross bedded quartzite with pebbly sandstone beds.|13-JAN-23
25778|Beasley River Quartzite|69003|5|Briefly described|p7-8|||Ashburton Basin. Wedge top to marginal foredeep deposits. c.300m thick.||||Unconformably overlies Kazput Formation. Is overlain conformably by Cheela Springs Basalt.|Fluvial to shallow-marine sandstones and conglomerates.|
25778|Beasley River Quartzite|69028|5|Briefly described|Map Legend|Orosirian|Rhyacian|Ashburton and Blair Basins. Mapped with Cheela Springs Basalt and Wooly Dolomite as a single unit.||Of the Wyloo Group, lower.|||Conglomerate, sandstone, mudstone, basalt, chert, and locally stromatolitic dolomite.|07-MAY-14
25778|Beasley River Quartzite|69080|5|Briefly described|p688|||Deposited during 2215-2145 Ma Ophthalmian Orogeny.||Unit in Wyloo Group.|Coeval with deposition of Moogie Metamorphics.|||
25778|Beasley River Quartzite|69166|6|Mentioned|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|||Wyloo Group||||
25778|Beasley River Quartzite|69185|5|Briefly described|500k_geologyp08_lut.csv||Paleoproterozoic|Of Ashburton Basin.||Unit of Wyloo Group.||||
25778|Beasley River Quartzite|69538|6|Mentioned|p517 Fig.3, p533|Paleoproterozoic|Paleoproterozoic|||Unit in Wyloo Group.||||
25778|Beasley River Quartzite|69565|6|Mentioned|p133 Fig.1|||Hamersley Province.||Wyloo Group.||Overlies Kazput Formation (Turee Creek Group). Is overlain by Cheela Springs Basalt.||
25778|Beasley River Quartzite|69569|6|Mentioned|p285 Fig.1|||East Pilbara Terrane.||Wyloo Group, Lower.||||
25778|Beasley River Quartzite|69583|6|Mentioned|p132|||Probably time-equivalent to the (c.2240-2145 Ma) Moogie Metamorphics.||Wyloo Group.||||
25778|Beasley River Quartzite|69745|6|Mentioned|p271, 273, 275, 287|||Hamersley Province. Presented as Beasley River formation on pp275, 287. See also references to Beasley Quartzite (p270, 286).|c.2150 Ma.|Lower Wyloo Group.|||Quartzites.|
25778|Beasley River Quartzite|69754|6|Mentioned|p316-p317, p340|||Pilbara Craton.||Wyloo Group|Includes the Three Corners Conglomerate Member and the Nummana Member.|||
25778|Beasley River Quartzite|70086|5|Briefly described|p196|Paleoproterozoic|Paleoproterozoic|Geological province: Pilbara Craton. Of the Hamersley Basin.||Unit of Wyloo Group.|Includes Nummana Member and Three Corners Conglomerate Member.|Overlain by Cheela Springs Basalt. Underlain unconformably by Kazput Formation/Turee Creek Group/Mount Bruce Supergroup.||
25778|Beasley River Quartzite|70327|5|Briefly described|p1-2, p4, p10-11, p16-17|||Horseshoe Basin. Up to 360m thick. Locally tightly folded.||||Is overlain conformably by Cheela Springs Basalt and unconformably by Mount McGrath Formation.|Fluvial and shallow-marine siliciclastic sandstones.|
25778|Beasley River Quartzite|70795|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|West Australian Craton, Turee Creek Basin|2208 Ma||||Fine to coarse grained, silicified quartz sandstone; minor conglomerate and siltstone; intruded by dolerite sills.|
25778|Beasley River Quartzite|70814|6|Mentioned|p70|||||Shingle Creek Group||||
25778|Beasley River Quartzite|70949|5|Briefly described|p988-989|Paleoproterozoic|Paleoproterozoic|||Shingle Creek Group.|||Quartz sandstone.|
25778|Beasley River Quartzite|70958|5|Briefly described|p3, 4, Fig. 1|Paleoproterozoic|Paleoproterozoic|||Of Wyloo Group||Overlain by Cheela Springs Basalt.||
25778|Beasley River Quartzite|71112|4|Described|p69-71,75-80,82-83,88|Rhyacian|Rhyacian|Geological province: Ashburton Province, Pilbara Craton. Of the Horseshoe Basin (intracontinental rift basin). Fan deltaic succession. Deeply incised into underlying Turee Creek Group. Mixed fluvial and shallow-marine depositional environments, with subaerially emplaced basalts and subvolcanic dolerite sills (which may be subvolcanic to Cheela Springs Basalt). Youngest zircon provenance for all samples combined for the Beasley River Quartzite are 2276+\-41 Ma. Potentially deposited over a span of less than 3myr.|<2208+\-10 Ma||Includes Three Corners Bore Conglomerate.|Overlain by Cheela Springs Basalt. Underlain unconformably by Turee Creek Group.|Siliciclastic sandstones and mudrocks, basalt flows and subvolcanic dolerite sills.|
25778|Beasley River Quartzite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
25778|Beasley River Quartzite|71550|4|Described|p34-40,42-45,47|Rhyacian|Rhyacian|Geological province: Of Hamersley Basin. Depositional environment: interbedded fluvial and aeolian facies. Krapez et al. (2017) presented maximum age of 2.33 Ga. U-Pb zircon analysis of quartz-rich sandstone from this study yield maximum age of 2.33 Ga (2336+\-13 Ma). Detrital provenance is likely from erosive products of underlying Hamersley Province and Pilbara basement, or potentially from the Glenburgh Terrane.||Unit of lower Wyloo Group.||Overlain by Cheela Springs Basalt. Underlain unconformably by Kazput Formation/Turee Creek Group.|Massive basal fluvial conglomerate and overlain by a unit of greenish fine-grained quartz-rich sandstone.|03-SEP-19
25778|Beasley River Quartzite|71808|6|Mentioned|p48, p50, p149, p156|||||||Overlain by the Cheela Springs Basalt.||
25778|Beasley River Quartzite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Turee Creek Basin.||Shingle Creek Group|||Fine- to coarse-grained, silicified quartz sandstone; ferruginous conglomerate, sandstone, and pebbly sandstone; siltstone and dolostone; intruded by Balgara Dolerite sills.|
25778|Beasley River Quartzite|72570|6|Mentioned|p2|||||Shingle Creek Group||Overlain by the Cheela Springs Basalt. Unconformably overlies the Turee Creek Group.||
25778|Beasley River Quartzite|72712|4|Described|p5-7, p9, p19-p25, p29-35.|Rhyacian|Rhyacian|The Beasley River Quartzite has a measured thickness of about 280 m in the Hardey Syncline, which includes at least one dolerite sill in the upper third of the formation. The unit is c. 400m thick in type section c.45 km to W. Facies analysis identified two, generally upwards-fining cycles, interpreted as the product of uplift-induced alluvial fan progradation followed by tidal shoreline and offshore sedimentation during subsidence and slow coastal retreat. Other workers have suggested the units is entriely fluvial- eolian. See also p23, p24, p36 Fig.25, p42, p43-45, p47-49, p52-53, p55-56.|U-Pb SHRIMP MDA < 2276+/-41 Ma|Shingle Creek Group|Three Corner Conglomerate Member.|Unconformably overlies Anthiby Formation. Intruded by Balgara Dolerite.|Medium- to coarse grained white quartzite and quartz arenites that locally contains a basal conglomerate of variable thickness comprising BIF and hematite-ore pebbles. Includes sandstone and conglomerate.|
25778|Beasley River Quartzite|72758|5|Briefly described|p4 Fig.1, p14 Tb.1, p31-32.|Paleoproterozoic|Paleoproterozoic|Overlies Mount Bruce Supergroup with angular unconformity. Max. thickness 360m. Predominantly shallow marine shelf deposits, with localized alluvial fan sediments at the base.||Wyloo Group|Includes Three Corner Conglomerate Member.|Unconformably overlies Turee Creek Group, Hamersley Group, Fortescue Group. and underlies Cheela Springs Basalt.|Cream or white-weathering, silicified quartz sandstone, local BIF-derived conglomerate, mudstone, and carbonate. The lower parts of this unit includes sandstone and quartz sandstone.|
25778|Beasley River Quartzite|73538|6|Mentioned|p2 Fig. 1B, p3-4|Orosirian|Rhyacian|Basal unit of the Wyloo Group.|Between ca 2210 Ma and 2031 +/- 6 Ma|Wyloo Group, Lower||Unconformably underlain by the Turee Creek Group including the Kazput Formation. Overlain by Cheela Spring Basalt.|Quartzite.|
74911|Beaton Creek Member|64653|5|Briefly described|Map Legend|Archean|Archean|Of Hardey Formation. Geological Province: Pilbara Craton. Pebble to cobble conglomerate interbedded with medium- to coarse-grained sandstone.||||||07-FEB-11
74911|Beaton Creek Member|65008|5|Briefly described|p22, p29, p41|Neoarchean|Neoarchean|Originally referred to as the Beatons Creek Conglomerate by Noldart and Wyatt (1962). Contains significant placer gold mineralisation.||Of the Hardey Formation||Underlain conformably by the Mosquito Creek Formation.|Comprises very coarse-grained lenticular conglomerate with rounded to subangular pebbles and cobbles of granitic and wacke lithic fragments.|03-FEB-17
74911|Beaton Creek Member|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Hardey Formation|||Polymictic conglomerate interbedded with medium- to coarse-grained sandstone|
74911|Beaton Creek Member|69590|4|Described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Of Northeast Pilbara Sub-basin; Marble Bar Sub-basin, Fortescue Basin. Events: Pilbara Craton breakup.|2766-2749 Ma (inferred)|Unit of Hardey Formation.|||Polymictic conglomerate interbedded with medium- to coarse-grained sandstone|
30234|Beatty Park Member|12099|6|Mentioned|p683|Orosirian|Orosirian|||Unit in Wilthorpe Formation.||||04-MAR-13
30234|Beatty Park Member|22694|5|Briefly described|p7|||Wilthorpe Formation.||||||15-DEC-08
30234|Beatty Park Member|22940|4|Described|Fig.6 p14, Tb2 p12|Paleoproterozoic|Paleoproterozoic|U-Pb zircon age 1996+/-35 Ma (Nelson, 1997). See also p10. Of Wilthorpe Formation, Padbury Group.||||||15-DEC-08
30234|Beatty Park Member|23744|4|Described|p17|Paleoproterozoic|Paleoproterozoic|See also page 24. Of Wilthorpe Formation. Geological Province: Padbury Basin.||||||07-NOV-08
30234|Beatty Park Member|23747|5|Briefly described|p4|Paleoproterozoic|Paleoproterozoic|Age: 1996+/-35 Ma (SHRIMP U-Pb). Of Padbury Group. Geological Province: Padbury Basin.||||||07-NOV-08
30234|Beatty Park Member|23749|5|Briefly described|p3 table 1|Proterozoic|Proterozoic|Of Wilthorpe Formation. Geological Province: Padbury Basin.||||||
30234|Beatty Park Member|43831|5|Briefly described|Map Legend||Paleoproterozoic|Padbury Basin.||||||15-DEC-08
30234|Beatty Park Member|49896|5|Briefly described|p3 Tb. 2|||||||||
30234|Beatty Park Member|50222|5|Briefly described|p320 Fig. 3, p327|Paleoproterozoic|Paleoproterozoic|Of the Wilthorpe Formation (Padbury Group). Contains lithic fragments derived from mafic rocks of the Narracoota Formation. Geological Province: Padbury Basin.||||||15-DEC-08
30234|Beatty Park Member|63866|5|Briefly described|p164|||SHRIMP age is interpreted as constraining the maximum depositional age for this member.|1996 +/- 35 Ma (SHRIMP U-Pb)|||Overlies the Labouchere Formation||
30234|Beatty Park Member|64580|4|Described|map legend||Paleoproterozoic|Of Wilthorpe Formation. Chloritic siltstone; sandstone; and breccia; numerous mafic volcanic fragments.||||||15-DEC-08
30234|Beatty Park Member|65408|5|Briefly described|p83.|Paleoproterozoic|Paleoproterozoic|||Unit in Wilthorpe Formation.|||Mafic wacke conglomerate.|17-JAN-12
30234|Beatty Park Member|65411|5|Briefly described|pp88-89.|Paleoproterozoic|Paleoproterozoic|Local equivalent of Heines Member. REE geochemical analyses suggest that the mafic epiclasts are derived from nearby uplifted blocks of the Narracoota Formation.||Unit in Wilthorpe Formation.||Conformably overlies Labouchere Formation. Is overlain conformably by, and grades into, Robinson Range Formation.|Volcanic-derived mafic clastic rocks intercalated with white chert beds towards the top.|
30234|Beatty Park Member|65419|2|Defined|p37, p38, pp43-45.|Paleoproterozoic|Paleoproterozoic|Defined in this study. No type section; type area is the Mount Padbury - Beatty Park Bore area. Corresponds to that part of the Labouchere Formation of Elias et al. (1980) that outcrops on Padbury 1:100 000 sheet, (a) adjacent to the Robinson Range Formation in the Mount Padbury-Beatty Park Bore area and (b) to the NE adjacent to the Labouchere and Robinson Range Formations. Named after Beatty Park Bore. Maximum depositional U-Pb age, from detrital zircons. Thickness is estimated to exceed 470 m. Lateral equivalent to the Heines Member.|1996 +/- 35 Ma (Nelson, 1997).|Unit in Wilthorpe Formation.||Conformably overlies Labouchere Formation. Is faulted against the Narracoota Formation. Is overlain conformably and gradationally by Robinson Range Formation.|Finely-laminated, well-bedded shale-siltstone layers that mainly contain quartz and chlorite; lithic wacke, polymictic conglomerate and breccia which all contain fragments of basalt, mafic schist, chert and chlorite-quartz wacke; white chert lenses.|
30234|Beatty Park Member|65896|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Member of Wilthorpe Formation, Padbury Group. Fine to very fine grained shale to sandstone with breccia layers containing fragments of quartz wacke and massive chlorite rock; intercalated thin chert layers towards the top; metamorphosed.||||||
30234|Beatty Park Member|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic|||Wilthorpe Formation|||Chloritic siltstone; sandstone; and breccia; numerous mafic volcanic fragments|
30234|Beatty Park Member|69003|5|Briefly described|p16|||Padbury Basin.||Wilthorpe Formation.|||Turbidites.|
30234|Beatty Park Member|69166|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|||Wilthorpe Formation|||Chloritic siltstone; sandstone; and breccia; numerous mafic volcanic fragments.|
30234|Beatty Park Member|69596|6|Mentioned|p10|||Padbury Basin.||Wilthorpe Formation.||||
30234|Beatty Park Member|70804|4|Described|p2-p3, p18-p19, p21, p42, plate 1||Orosirian|Outcrops in Mount Padbury area on PADBURY and contains clastic rocks sourced from the Narracoota Formation. SHRIMP age is derived from a chert lense directly underlying this unit and therefore provides a maximum depositional age.|<1996 +/- 35 Ma (SHRIMP U-Pb) |Wilthorpe Formation||Overlies the Narracoota Formation. Conformably overlain by the Robinson Range Formation.|Metamorphosed chlorite-quartz shale, siltstone and wacke with several conglomeratic or breccia lenses and finely laminated chert layers in places.|27-FEB-23
30234|Beatty Park Member|71484|5|Briefly described|p130|||Geological province: Of Padbury Basin. Misspelt as Beattie Park Member on p138.||Unit of Wilthorpe Formation.||Overlain by Robinsons Range Formation.||30-AUG-19
28358|Becher Sand|12759|4|Described|p49; p28 Tb. 7; p32 Fig 15; P36 Fig 17|Quaternary||Defined Semeniuk and Searle (1985). Type section near coast at Woodman Point, 19 km SW of Perth. Max thickness 20m at Rockingham. Near-shore marine origin.||Of Kwinana Group||Overlies Tamala Limestone unconformably and is unconformably overlain by Safety Bay Sand (this study).|Fine- to medium-grained quartz and skeletal sand, mostly structureless and bioturbated; lenses of silty calcareous clay, rich in shell fragments.|12-MAY-14
28358|Becher Sand|40400|2|Defined|p109, p111|Holocene|Holocene|Overlies Tamala Lst, Cooloongup Sand, Leschenault Fm. Age: <7,000yrs.  Thickness: >20m. Geol.Prov: Perth Basin. Sequence of grey structureless to bioturbated, fine and medium quartzo-skeletal sand with lesser muddy sand, layered mud and seagrass peat.||||||06-AUG-07
28358|Becher Sand|40731|5|Briefly described|p34|||||||||
28358|Becher Sand|41200|5|Briefly described|p25, p27|||Conformably overlies Bridport Calcilutite. Shallow water deposits, bioturbated to shelly quartzo-skeletal sand and muddy sand.||||||06-AUG-07
28358|Becher Sand|41342|6|Mentioned|p22|||||||||
28358|Becher Sand|41502|4|Described|Table 1|||||||||
28358|Becher Sand|41783|4|Described|p48|||||||||
28358|Becher Sand|61521|5|Briefly described|p4 Tb.1, p40, p39 Tb.7|Holocene|Holocene|Grey quartzo-skeletal carbonate muddy sand with seagrasses. Formerly part of Saftey Bay Sand, which was divided into a beach and a seagrass bank suite. Overlain by Safety Bay Sand; overlies basin muds of Cockburn Sound. Geol. Prov: Rottnest Shelf region.||||||07-FEB-08
28358|Becher Sand|63330|5|Briefly described|p192|Quaternary|Quaternary|Geological Province: Perth Basin/Swan Coastal Plain.||||||31-JAN-08
28358|Becher Sand|63745|6|Mentioned|p64 Fig. 3|||||||||07-FEB-11
28358|Becher Sand|68811|5|Briefly described|p90, p181|Quaternary|Neogene|One of a group of 'superficial sediments' described as being up to 90m thick.|||||Group description: Sand, limestone, silt and clay.|21-JAN-22
26376|Bedford Sandstone|22547|6|Mentioned|p21|||Of the Speewah Group. Geological province: Speewah Basin.||||||14-NOV-06
26376|Bedford Sandstone|22754|5|Briefly described|p10 Tb. 2|Paleoproterozoic|Paleoproterozoic|Of the Speewah Group.||||||07-NOV-08
26376|Bedford Sandstone|23751|4|Described|p21|Paleoproterozoic|Paleoproterozoic|Of Speewah Group. Geological Province: Speewah Basin. Max. thickness: 500 m.||||||07-NOV-08
26376|Bedford Sandstone|42710|5|Briefly described|map legend|Proterozoic||||||||
26376|Bedford Sandstone|42811|5|Briefly described|p22|||of Speewah Group||||||
26376|Bedford Sandstone|43281|5|Briefly described|Map legend||Proterozoic|of Speewah Group.||||||
26376|Bedford Sandstone|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
26376|Bedford Sandstone|44230|5|Briefly described|Map Legend||Proterozoic|||||||
26376|Bedford Sandstone|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Speewah Group. White to pale brown, well sorted quartz sandstone. Age: c.1835Ma. Geological Province: Speewah Basin.||||||07-NOV-08
26376|Bedford Sandstone|44868|5|Briefly described|Map Legend||Proterozoic|||||||
26376|Bedford Sandstone|60714|5|Briefly described|p111-116, p118, p120-121. |Orosirian|Orosirian|500m thick unit formerly within King Leopold Sandstone but separated after discovery of a low-angle unconformity below a conglomerate facies within that unit (Williams 1969). Detailed stratigraphy.|c.1820 Ma.|Topmost unit of the Speewah Group.||Overlies Luman Siltstone. Is intruded by Hart Dolerite. Is overlain unconformably by King Leopold Sandstone (Kimberley Group).|Lowest 100 m comprise white to pale red, medium- to coarse-grained, well-sorted quartzarenite; next 400 m consists of bands of granule sandstone, pebble conglomerate, pale red, poorly sorted, coarse-grained feldspathic sandstone.|
26376|Bedford Sandstone|60844|5|Briefly described|pp15-16.|Late Paleoproterozoic|Late Paleoproterozoic|Newly named. Of the Speewah Group. The low-angle unconformity surface at the top of this unit shows numerous linear, parallel grooves, interpreted as Nye channels,  trending east-west; cutting across cross-strata and joints and infilled with overlying King Leopold Sandstone. Other erosional features include crescent-shaped hollows (sichelwannen), ridges and potholes, and smoothed surfaces. All these indicate a glaciated erosion surface, which in turn indicates a period of glaciation at odds with the claimed Proterozoic non-glacial interval.||Topmost unit in Speeewah Group.||Is unconformably (1 - 2 degrees) overlain by King Leopold Sandstone.||21-JAN-15
26376|Bedford Sandstone|64748|4|Described|p268, p269 Fig 2, p269 Tb.1, p270|||At the top of the Speewah Group; unconformably/disconformably underlies the King Leopold Sandstone (Emu Point Member);overlies the Luman Siltstone; medium- to coarse-grained cross-bedded feldspathic sandstone;||||||21-JUL-15
26376|Bedford Sandstone|67563|6|Mentioned|p122 Fig.2|||||Of the Speewah Group.||||21-JUL-15
26376|Bedford Sandstone|68078|5|Briefly described|p6 figure 3, p8, p23|Paleoproterozoic|Paleoproterozoic|||Speewah Group||Overlies Valentine Siltstone, Unconformably/disconformably overlain by King Leopold Sandstone|Sandstone.|13-SEP-22
26376|Bedford Sandstone|68992|6|Mentioned|p498 Fig.1|||Speewah Basin.||Of the Speewah Group.||||
26376|Bedford Sandstone|69003|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|||Speewah Group.||Overlies Luman Siltstone. Is overlain unconformably by King Leopold Sandstone.||
26376|Bedford Sandstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Speewah Basin. Unit relationships from geochron file 182105.1.pdf.||Speewah Group||Unconformably overlain by King Leopold Sandstone, Kimberley Group.|White to pale brown, well-sorted quartz sandstone.|30-JUL-15
26376|Bedford Sandstone|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Speewah Group|||White to pale brown, well sorted quartz sandstone.|
26376|Bedford Sandstone|69585|6|Mentioned|p4-5|Orosirian|Orosirian|Western Lamboo Province.||Speewah Group.||||
26376|Bedford Sandstone|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Speewah Basin. Events: King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1; King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1. See also geochron files.|1835-1784 Ma (Inferred)|Unit of Speewah Group.||Overlain unconformably by King Leopold Sandstone/Kimberley Group.|White to pale brown, well-sorted quartz sandstone|
26376|Bedford Sandstone|70154|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1797-1835 Ma||||White to pale brown, well sorted quartz sandstone.|
26376|Bedford Sandstone|70812|5|Briefly described|p6|Orosirian|Orosirian|Western Zone of the Halls Creek Orogen, Lamboo Province.|c. 1850-1800 Ma|Speewah Group||||
26376|Bedford Sandstone|70851|5|Briefly described|p4|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province.|c. 1850-1800 Ma|Speewah Group||Overlies the Luman Sandstone. Overlain by the King Leopold Sandstone.|Sedimentary rocks.|28-MAR-23
26376|Bedford Sandstone|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen, King Leopold Orogen. Of Speewah Basin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv , 1M_geologyp12_lut.csv.|1835-1797 Ma (inferred)|Unit of Speewah Group.||Uppermost unit of Speewah Group. Overlain unconformably by King Leopold Sandstone.|Siliceous argillaceous and slightly feldspathic quartz sandstone with sparse quartz, chert and claystone pebbles and ubiquitous large scale cross beds; basal red-purple-brown medium grained quartzite and flaggy micaceous fine sandstone|
26376|Bedford Sandstone|71281|4|Described|p421|Paleoproterozoic|Paleoproterozoic|Griffin et al. (1993). Speewah Basin. Up to 500m thick.||Speewah Group.||Overlies Luman Siltstone. Is overlain by King Leopold Sandstone (Kimberley Group).|Argillaceous and feldspathic sandstone hosting a few quartz, chert and claystone pebbles and showing large-scale cross-beds. There is a basal red-purple-brown, medium-grained quartzite and thin interbeds of flaggy micaceous fine sandstone.|
26376|Bedford Sandstone|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Speewah Group.||Overlies Lansdowne Arkose. Is overlain by Hart Dolerite.|White to pale brown sandstone and conglomerate.|
26376|Bedford Sandstone|72490|5|Briefly described|p3-4|||Maximum thickness of 500 m.||Speewah Group|||Argillaceous and feldspathic quartz sandstone containing minor quartz, chert and claystone pebbles and showing large-scale cross-beds; basal red-purple-brown medium-grained quartzite and thin interbeds of flaggy micaceous fine sandstone.|
31125|Bedout Formation|13255|6|Mentioned|p369|Early Jurassic|Late Triassic|Roebuck Basin.||||Unconformably overlies Keraudren Formation. Is overlain by Depuch Formation.||
31125|Bedout Formation|43173|5|Briefly described|12-54||Triassic|||||||
31125|Bedout Formation|43705|6|Mentioned|p20|Early Jurassic|Middle Triassic|||||||
31125|Bedout Formation|62837|5|Briefly described|Stratigraphic columns|Early Jurassic|Late Triassic|Age: 220-~203Ma. Geological Province: Bedout Sub-basin and Bedout High (Roebuck Basin).||||||
31125|Bedout Formation|69297|6|Mentioned|p337, p352|Rhaetian|Rhaetian|Canning and Roebuck Basins. ||||Overlies the Upper Keraudren Formation. Overlain by the Murat Siltstone or the Depuch Formation.||
31125|Bedout Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Roebuck Basin.||||Overlies Brigadier Formation. Is overlain by Dupuch Formation.||
31125|Bedout Formation|70065|5|Briefly described|Rowley: Fig.2; p2. Regional: Fig.4; p3-4|Rhaetian|Rhaetian|Roebuck Basin and offshore Canning Basin. Transgressive shales form intraformational seals.||||Overlies Upper Keraudren Formation. Is overlain by Depuch Formation or Murat Siltstone. Equivalent to Brigadier Formation.||
29989|Bee Gorge Member|22682|4|Described|p29|Archean|Archean|2603 +/- 7 Ma on zircon. Disconformably overlain by Mount Sylvia Formation||||||03-MAR-10
29989|Bee Gorge Member|22689|6|Mentioned|138,139|Paleoproterozoic|Archean|Wittenoom Formation, Hamersley Basin. Age 2416 Ma||||||07-NOV-08
29989|Bee Gorge Member|22701|4|Described|p37|Siderian|Siderian|Also Fig2, p39. Wittenoom Formation, Hamersley Basin. 2346 +/- 38 Ma. Overlies Paraburdoo Member, overlain by Mount Sylvia Formation.||||||02-MAR-15
29989|Bee Gorge Member|23612|5|Briefly described|p843|||Of Wittenoom Formation.||||||
29989|Bee Gorge Member|23890|5|Briefly described|p9|Paleoproterozoic|Archean|Of Wittenoom Formation, Hamersley Group. Geological Province: Hamersley Basin.||||||07-NOV-08
29989|Bee Gorge Member|24041|5|Briefly described|p495|Archean|Archean|Of Wittenoom Formation.  Geological Province: Pilbara Craton.||||||07-APR-09
29989|Bee Gorge Member|24544|4|Described|p57 Fig.43|Archean|Archean|Of Wittenoom Formation. Overlies Paraburdoo Member. Overlain by Mount Sylvia Formation. Age: 2561 Ma. Geological Province: Hamersley Basin.||||||07-NOV-08
29989|Bee Gorge Member|43064|3|Fully described|p68|||Of Wittenoom Formation.||||||07-APR-09
29989|Bee Gorge Member|43290|5|Briefly described|p6||Archean|of Wittenoom Formation.(Simonson et al ;1993)||||||07-NOV-08
29989|Bee Gorge Member|60373|6|Mentioned|p145 Tb. 1|Archean|Archean|Of Wittenoom Formation.||||||23-JUN-09
29989|Bee Gorge Member|60706|5|Briefly described|p623 Fig.2, p644 App.1|Archean|Archean|Of the Wittenoom Formation. Age: 2565+/-9 Ma (SHRIMP). Geological Province: Hamersley Basin.||||||07-NOV-08
29989|Bee Gorge Member|61560|5|Briefly described|p498 Tb. 4|||Of the Wittenoom Formation. Displays impact spherules caused by impact ejecta. Geological Province: Hamersley Basin.||||||
29989|Bee Gorge Member|61575|5|Briefly described|p760 |Neoarchean|Neoarchean|Of the Wittenoom Formation; contains a spherule layer  interpreted as impact-generated melt.||||||07-NOV-08
29989|Bee Gorge Member|61576|4|Described|p773|Neoarchean|Neoarchean|Of Wittenoom Formation. Argillite, dolomite, limestone, banded iron-formation, chert, volcaniclastics. Neoarchaean impact sperules. Overlies Paraburdoo Member. Age: 2561+/-8Ma, 2541+18/-15Ma.  Geol. Prov: Hamersley Basin.||||||07-NOV-08
29989|Bee Gorge Member|61577|5|Briefly described|p787 Tb. 1|Archean|Archean|Of the upper Wittenoom Formation. Age: ca2.56Ga.  Geological Province: Hamersley Basin.||||||07-NOV-08
29989|Bee Gorge Member|62129|3|Fully described|p9|Archaean|Archaean|Of Wittenoom Formation. Thickness: 230m. Geological Province: Hamersley Basin. Thinly laminated graphitic argillite is the main lithology, together with subordinate thicknesses of carbonate, chert, volcaniclastic rock and iron-formation.||||||07-FEB-11
29989|Bee Gorge Member|65757|5|Briefly described|p81 Tb.2, p84 Fig.2|||in the upper Wittenoom Formation, carbonate turbidite, overlies the Mount Newman Formation||||||
29989|Bee Gorge Member|65829|5|Briefly described|p25.|Neoarchean|Neoarchean||2561 +/- 8 Ma (Trendall et al. 1998).|Unit in Wittenoom Formation.|||Includes a crystal-rich tuffaceous shale.|
29989|Bee Gorge Member|66882|5|Briefly described|p118|Neoarchean|Neoarchean|Hamersley Group. [Mis-spelled as Bee George]. Detrital zircons of the same age occur in Cook Gap Schist, Gawler Craton.|2561+/-8 Ma and 2565+/-9 Ma||||Includes tuffaceous units.|
29989|Bee Gorge Member|67130|5|Briefly described|p3 fig 2|Neoarchean|Neoarchean||2565 Ma - 2541 Ma + 18 Ma /- 15 Ma|Wittenoom Formation||Overlies Paraburdoo Member, Overlain by Mount Sylvia Formation|Shale|
29989|Bee Gorge Member|67201|4|Described|p34 Fig.18, p51|||Thickness 150-250 m.|c. 2565 Ma SHRIMP U-Pb zircon Trendall et al. 2004|Wittenoom Formation|||Includes BIF.|
29989|Bee Gorge Member|67721|5|Briefly described|p37|Neoarchean|Neoarchean|Geochronology from tuffaceous units by Trendall et al. (1998, 2004). Approximately 140 m thick.|c. 2561 +/- 8 Ma; 2565 +/- 9 Ma|Of the Wittenoom Formation.|||Turbiditic calcareous shales, minor chert, banded iron formation.|
29989|Bee Gorge Member|68035|4|Described|p292 Fig 6|Neoarchean|Neoarchean|Hamersley Group, Hamersley Basin.|2565 - 2541 +18/-15 Ma (Pb-Pb carbonate)|Of Wittenoom Formation.||Overlies Paraburdoo Member, Overlain by Mount Sylvia Formation.|Shale.|
29989|Bee Gorge Member|68280|6|Mentioned|p5, p38|||||Wittenoom Formation, upper part|||Shale, spherules in a carbonate-siltstone matrix.|13-JAN-23
29989|Bee Gorge Member|69538|6|Mentioned|p517 Fig.3, p529-530, p574-575, p583-585|||Appears as Bee George Member in Fig.3.||Unit in Wittenoom Formation.||||
29989|Bee Gorge Member|69563|5|Briefly described|p690-691|||Contains a spherule marker bed.|2562 +/- 6 Ma. |Unit in Wittenoom Formation.||||
29989|Bee Gorge Member|71550|6|Mentioned|p45|||Geological province: Of Hamersley Basin.||Unit of Wittenoom Formation.||||03-SEP-19
29989|Bee Gorge Member|71808|4|Described|vii, p2, p23-p24, p26|||Hamersley Province. Sedimentary structures includes intraclasts, flat-pebble conglomerates, cross-bedding, ripples, concretions and roll-ups. Thickness varies regionally from 210m in the northwest to an average of 140m in the central and southeast parts of the province. Unique for high energy sediments within the Hamersley Group. See also p101-p102, p105, p117, p132, p177, p182, p239.||Wittenoom Formation||Overlain by the Mount Sylvia Formation.|Thinly-bedded, fissile turbiditic shale and dolomitic shales with subordinate carbonate and chert beds.|
29989|Bee Gorge Member|72493|5|Briefly described|p30|||Hamersley Basin.||Wittenoom Formation.||Overlies Paraburdoo Member. Is overlain by Mount Sylvia Formation.|Shale.|
29989|Bee Gorge Member|72569|5|Briefly described|p2, 5, 16|||Of the Hamersley Basin.||Wittenoom Formation||Overlies Paraburdoo Member.||
29989|Bee Gorge Member|73022|5|Briefly described|p3, p4 Fig.3-4, p5 Fig.5-6, p7 Fig.9|Neoarchean|Neoarchean|Some ferruginous chert beds contain greenalite nanoparticles, syneresis structures and shrinkage structures indicting a depositional origin from hydrothermal vent plumes.|2.58 Ga|Wittenoom Formation|Main Tuff Interval|Overlies the Paraburdoo Member, underlies the Mount Sylvia Formation.|Shale, minor ferruginous chert and banded iron formation, felsic tuff in the Main Tuff Interval. Includes laminated chert intercalated with fine-grained marine carbonate and siliciclastic siltstone and shale.|
29989|Bee Gorge Member|73290|6|Mentioned|p784|||Hamersley Province.||||||
29989|Bee Gorge Member|73538|6|Mentioned|p4|||||Wittenoom Formation||Underlain by the Paraburdoo Member. Overlain by the Mount Sylvia Formation.|Mudstone/siltstone.|
24706|Bee Hill Sandstone|30881|4|Described|p527|||||||||
24706|Bee Hill Sandstone|34135|4|Described|Table 1|||Middle Proterozoic. See also PP13,14,15||||||
24706|Bee Hill Sandstone|36884|6|Mentioned|p156|||||||||
24706|Bee Hill Sandstone|37460|5|Briefly described|p122|||||||||
24706|Bee Hill Sandstone|39697|6|Mentioned|p14|||||||||
24706|Bee Hill Sandstone|40089|4|Described|p58|||||||||
24706|Bee Hill Sandstone|41669|6|Mentioned|p36|||||||||
24706|Bee Hill Sandstone|44297|14|Not recorded|p.5,7,10-11|||(F51-9).||||||
24706|Bee Hill Sandstone|44298|14|Not recorded|map legend||Proterozoic|||||||
24706|Bee Hill Sandstone|44438|14|Not recorded|map legend||Mesoproterozoic|Part of Manganese Group. M.Proterozoic.||||||
24706|Bee Hill Sandstone|67183|5|Briefly described|Figs.3, 7, 21; p645 Tb.1, p647|Mesoproterozoic|Mesoproterozoic|Here reassigned to Stag Arrow Formation (p647) although the former name is used in the listed diagrams. Present in the south-western Oakover Basin.||||Overlies the Coondoon Formation.|Sandstone, siltstone, sedimentary breccia, conglomerate.|
31787|Beefwood Yard Granite|22547|4|Described|p11||Orosirian|Of the Paperbark supersuite.||||||14-NOV-06
31787|Beefwood Yard Granite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1850Ma. Geological province: Kimberley Province (East).||||||07-FEB-11
31787|Beefwood Yard Granite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
31787|Beefwood Yard Granite|43853|5|Briefly described|Map Legend||Proterozoic|||||||
31787|Beefwood Yard Granite|44230|5|Briefly described|Map Legend||Proterozoic|||||||
31787|Beefwood Yard Granite|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Paperbark Supersuite.||||||07-NOV-08
31787|Beefwood Yard Granite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Paperbark Supersuite|||Medium- and coarse-grained porphyritic biotite monzogranite.|30-JUL-15
31787|Beefwood Yard Granite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Paperbark Supersuite|||Medium and coarse grained porphyritic biotite monzogranite.|
31787|Beefwood Yard Granite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone.|1855-1855 Ma (Inferred)|Unit of Paperbark Supersuite.|||Medium- and coarse-grained porphyritic biotite monzogranite|
31787|Beefwood Yard Granite|70154|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1855 Ma|Paperbark Supersuite|||Medium-coarse grained porphyritic biotite monzogranite|
31787|Beefwood Yard Granite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1855 Ma (inferred)|Unit of Paperbark Supersuite.|||Medium- and coarse-grained porphyritic biotite monzogranite|
30579|Beekeeper Formation|5257|6|Mentioned|p153|Permian|Permian|Perth Basin. Of Hall & Kneale (1992) superseded by Beekeeper Member. ||||||
30579|Beekeeper Formation|12758|5|Briefly described|p8 Fig. 9|Permian|Permian| Geological Province: Northern Perth Basin.||||||
30579|Beekeeper Formation|14227|5|Briefly described|p7, p10|Ufimian|Kungarian|Mixed carbonate-siliciclastic marine unit. In the Beagle Ridge region.||||||07-FEB-11
30579|Beekeeper Formation|23279|4|Described|p15,18,20|Late Permian|Kungurian|(Hall and Kneale, 1992).||||||
30579|Beekeeper Formation|23520|5|Briefly described|p6 Fig. 4|Late Permian|Late Permian|Geological Province: Abrolhos Sub-basin.  See also p9.||||||
30579|Beekeeper Formation|24390|5|Briefly described|p15 Fig. 8|Permian|Permian|Geological Province: Perth Basin.||||||
30579|Beekeeper Formation|24443|5|Briefly described|Fig.30|Early Triassic|Late Permian|Unconformably overlies Carynginia Formation. Conformably overlain by Kockatea Shale. Geological Province: Bight Basin.||||||10-JAN-05
30579|Beekeeper Formation|43216|5|Briefly described|Map Legend||Permian|Perth Basin.||||||21-APR-08
30579|Beekeeper Formation|43297|6|Mentioned|p8||Late Permian|||||||
30579|Beekeeper Formation|43495|4|Described|6-32||Kazanian|||||||
30579|Beekeeper Formation|43504|4|Described|6-18|Kazanian|Kungurian|||||||
30579|Beekeeper Formation|50085|5|Briefly described|p15 Fig. 8|Permian|Permian|Geological Province: Northern Perth Basin.||||||11-MAY-04
30579|Beekeeper Formation|50107|5|Briefly described|Map legend|Permian|Permian|Geological Province: Northern Perth Basin.||||||
30579|Beekeeper Formation|50620|5|Briefly described|p200 Fig. 8|Late Permian|Late Permian|Geological Province: Perth Basin.||||||
30579|Beekeeper Formation|50621|5|Briefly described|p165 Fig. 6|Late Permian|Late Permian|Geological Province: Perth Basin.||||||
30579|Beekeeper Formation|60377|5|Briefly described|p61 Fig. 3|Wuchiapingian|Wordian|Overlain by Hovea Member of the Kockatea Shale. Geological Province: Perth Basin. Marine depositional environment.||||||07-FEB-11
30579|Beekeeper Formation|60386|5|Briefly described|p297, p313|Lopingian|Guadalupian|Northern Perth Basin. Limestone nearshore-shelf.  Age shown as ~Late Permian.||||Lateral equivalent (in part) of Dongara and Wagina Formations.||
30579|Beekeeper Formation|61023|5|Briefly described|p20 Fig 10|Permian|Permian|Geological Province: Perth Basin.||||||11-APR-08
30579|Beekeeper Formation|61546|6|Mentioned|p385 Fig.5.|Late Permian|Early Permian|||||||
30579|Beekeeper Formation|61811|5|Briefly described|p3 Fig.2, p39, p62.|Late Permian|Middle Permian|Northern Perth Basin. Lateral equivalent of Wagina Sandstone and of Dongara Sandstone to the north. Type section details in Appendix 1.||||Is unconformably overlain by Kockatea Shale.|Marine carbonates.|
30579|Beekeeper Formation|64635|5|Briefly described|p4 Fig.3, p23  |Wuchiapingian|Kungurian|||||Coeval with the Wagina and Dongara Sandstones.||
30579|Beekeeper Formation|64974|6|Mentioned|p144 Fig. 3|Kazanian|Ufimian|Geological Province: Perth Basin.||||||24-JUN-09
30579|Beekeeper Formation|67135|5|Briefly described|p5 Fig.7.|Permian|Permian|Perth Basin. Lateral equivalent of Dongara Sandstone to the north.||||Is overlain by Kockatea Shale.||
30579|Beekeeper Formation|67340|6|Mentioned|p6, 8, 25|Permian|Permian|Northern Perth Basin. Thermal rock properties.||||||
30579|Beekeeper Formation|67370|5|Briefly described|p318 Fig.10, p328.|Late Permian|Late Permian|Northern Perth Basin. Contains Wordian-Wuchiapingian microfossils. Cool, shallow-water ramp origin.|c.268 - 254 Ma.|||Is overlain by Wagina Sandstone.|Carbonates.|
30579|Beekeeper Formation|67925|6|Mentioned|Ch3 p15|||||||||
30579|Beekeeper Formation|69029|6|Mentioned|p332|Permian|Permian|Of Perth Basin.||||Overlain by Sabina Sandstone. Underlain by Dongara Sandstone.||
30579|Beekeeper Formation|69182|5|Briefly described|Ch2 p9, Ch2 p12, Ch2 p44-p45||Late Permian|Perth Basin. Deposited in a shallow marine environment. Potentially significant reservoir for the storage of carbon dioxide. See also  Ch2 p47, Ch2 p54-p55, Ch2 p57, Ch2 p60, Ch2 p64-p66, Ch2 p80, Ch2 p83-p84, Ch2 p91, Ch2 p92, Ch2 p94-p96, Ch2 p98, Ch2 p100, Ch2 p102, Ch2 p104, Ch2 p106, Ch2 p108, Ch2 p110.||||Equivalent to the Dongara Sandstone and the Wagina Sandstone.|Bio-clastic limestones.|
30579|Beekeeper Formation|70097|5|Briefly described|p20 Fig.4|Wordian|Wordian|Northern Perth Basin. Dandaragan Trough.|||||Limestone.|
30579|Beekeeper Formation|70128|5|Briefly described|p449|Permian|Permian|Northern Perth Basin.||||Conformably overlies Carynginia Formation. Is overlain unconformably by Kockatea Shale.||
30579|Beekeeper Formation|70774|5|Briefly described|p5 fig 3|Dorashamian|Kazanian|Northern Perth Basin.||||Equivalent to the Dongara Sandstone and the Wagina Sandstone.||
30579|Beekeeper Formation|71146|5|Briefly described|p6, p36,  p43 fig 33|Guadalupian|Guadalupian|Perth Basin.||||Overlies the Carynginia Formation. Overlain by the Wagina-Dongara Sandstone.|Carbonate and mudstone.|
30579|Beekeeper Formation|71623|4|Described|p347, 349, 355, 357,358,359,345,350,354||Roadian|Perth Basin. Some gas shows.||||Unconformably overlies Carynginia Formation. Correlated with Cody and Pearce Formations.|Limestone. Includes dolomitised thick crinoidal limestone in middle.|
30579|Beekeeper Formation|72258|5|Briefly described|p129,133-135|Lopingian|Guadalupian|Of Perth Basin. Neoarchean (2800-2600 Ma) detrital zircons attributed to Yilgarn Craton, along eastern boundary of Perth Basin (Kositcin et al., 2008; Mole et al., 2013; Nemchin and Pidgeon, 1997). Older material (3700-3000 Ma) probably also derived from Yilgarn Craton. Major peak in Mesoproterozoic (1300-1100 Ma) and minor Late Paleoproterozoic (1800-1600 Ma) detrital zircons correlate with characteristic ages and Hf isotopic signatures of magmatism in the Albany-Fraser-Wilkes Orogen (Clark et al., 2000; Fitzsimons, 2000, 2003; Kirkland et al., 2011; Spaggiari et al., 2015). Late Meso- to Early Neoproterozoic (1100-900 Ma) detrital zircons atributed to Pinjarra Orogen. Bimodal Neoproterozoic 750 and 500 Ma peaks in detrital zircon ages also likely to be derived locally from Pinjarra Orogen (p134-135 describes potential, but unlikely Gondwanan sources).||||Laterally gradees into Willespie Formation.||15-JAN-20
30579|Beekeeper Formation|72505|5|Briefly described|p890|Changhsingian|Wordian|Perth Basin. Correlates with Didecriletes ericanus and Dulhuntyispora parvithola zones.||||Overlain by and interfingers with the Dongara Sandstone. Overlain by the Kockatea Shale.||18-MAR-20
30579|Beekeeper Formation|72910|6|Mentioned|p4 Fig.3.|Late Permian|Late Permian|Shown as part of the Northern Perth Basin.||||Shown as underlying the Kockatea Shale and shown as being laterally equivalent to Dongara Sandstone.||
79240|Beekeeper Sequence|69297|6|Mentioned|p209, p225, p234, p238|||||||||
79240|Beekeeper Sequence|70097|6|Mentioned|p4|||In the Middle to Late Permian, was partly or totally removed by erosion from the Beagle Ridge and parts of the Abrolhos Sub-basin.||||||30-SEP-16
78593|Beenong Dyke Suite|65487|4|Described|p5, 7-9, p8 Fig. 3, p25-26 Fig. 13-14|||New name. Cuts the southern part of the Southern Cross Domain and Southwest Terrane of the South Yilgarn Craton. NW trending; moderately magnetic, relatively short in length. Mafic. Age unknown, but probably younger than c.1210 Ma, because they crosscut younger structures in the Kepa Kurl Booya Province near Bremer Bay. Composition unknown.||||||10-FEB-14
78593|Beenong Dyke Suite|68186|5|Briefly described|p30-31, Plate 1A|Phanerozoic|Proterozoic|Spaggiari et al. (2009). A set of NW-trending dykes, mostly moderately magnetic and relatively short in length. Age and composition unknown.|||||NW-trending mafic dykes; interpreted from aeromagnetic data.|
78593|Beenong Dyke Suite|69140|6|Mentioned|p3|||Geological province: Albany-Fraser Orogen.||||||
78593|Beenong Dyke Suite|69252|5|Briefly described|p65|||Spaggiari and Pawley (2012).||||Intrudes Recherche and Esperance Supersuites and Mount Ragged Formation.|Mafic dykes.|
78593|Beenong Dyke Suite|69412|6|Mentioned|p3 Fig.2|||Ravensthorpe area, Yilgarn Craton. SE- and ESE-trending dykes.||||||
78593|Beenong Dyke Suite|70023|6|Mentioned|p170|||Eastern Nornalup Zone and Madura Province.||||||
78593|Beenong Dyke Suite|70794|5|Briefly described|2_5m_interpdykel15_lut.csv|Neoproterozoic|Mesoproterozoic|Northwesterly trending; interpreted from aeromagnetic data.|1218- 541 Ma inferred||||Mafic dykes.|
78593|Beenong Dyke Suite|70802|5|Briefly described|GEOL_LUT_CSV files|Neoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen. Events: Western Australian events (4000-0.01 Ma). See 2_5m_interpdykel15_lut.csv, 250k_pre_mesozoic_interpgeol_lut.csv.|1218-541 Ma (inferred)||||Mafic dykes; northwesterly trending; interpreted from aeromagnetic data|
78593|Beenong Dyke Suite|70826|6|Mentioned|p14 tbl 5|Cambrian|Mesoproterozoic|South-east Yilgarn, Albany Fraser Orogen.1218-541 age range [range is quite large and not particularly useful]||||||
78593|Beenong Dyke Suite|71270|4|Described|2_5m_interpdykel15_lut.csv|Neoproterozoic|Mesoproterozoic|Geological province: Yilgarn Craton, West Australian Craton. Events: Western Australian events (4000 - 0.01 Ma).|1218-541 Ma (inferred)||||Mafic dykes; northwesterly trending; interpreted from aeromagnetic data|
28360|Behn Conglomerate|24061|6|Mentioned|p175|||Geological Province:  Canning Basin.||||||
28360|Behn Conglomerate|30525|6|Mentioned|Map legend|Frasnian|Givetian|Frasnian? to Givetian?||||||
28360|Behn Conglomerate|30533|4|Described|p24|||See also Table 6||||||
28360|Behn Conglomerate|31332|6|Mentioned|Fig. 3|||Frasnian||||||
28360|Behn Conglomerate|31870|6|Mentioned|p8|||||||||
28360|Behn Conglomerate|36890|4|Described|p335|||||||||
28360|Behn Conglomerate|39796|6|Mentioned|Map legend|Devonian|Devonian|||||||
28360|Behn Conglomerate|41158|6|Mentioned|Plate 2|||||||||
28360|Behn Conglomerate|41169|6|Mentioned|Fig.3|||||||||
28360|Behn Conglomerate|41215|6|Mentioned|p277|||||||||
28360|Behn Conglomerate|41730|6|Mentioned|p481|||||||||
28360|Behn Conglomerate|42030|6|Mentioned|p748|||||||||
28360|Behn Conglomerate|42710|5|Briefly described|map legend|Late Devonian||||||||
28360|Behn Conglomerate|42811|5|Briefly described|p43|||||||||
28360|Behn Conglomerate|43281|6|Mentioned|Map legend|Late Devonian|Late Devonian|Canning Basin||||||
28360|Behn Conglomerate|44998|14|Not recorded|p26,43|||(E51-8).||||||
28360|Behn Conglomerate|45101|6|Mentioned|Fig.8|||||||||
28360|Behn Conglomerate|45153|3|Fully described|App.3-36|||||||||
28360|Behn Conglomerate|66127|3|Fully described|pp143-146, p337, Plate 7. |Famennian|Late Frasnian|Of Guppy et al. (1958). Forms Mount Behn in central Napier Range. Northern Lennard Shelf. Thickness probably >330 m.||||Interfingers with Pillara Limestone. Grades up into Napier Formation.|Polymictic pebble, cobble and boulder conglomerate with lesser siltstone and coarse-grained, poorly sorted sandstone; alluvial-cone, fan-delta, and submarine-fan deposits.|
28360|Behn Conglomerate|69099|5|Briefly described|500k_geologyp08_lut.csv|Famennian|Frasnian|Frasnian and Famennian conglomerates associated with Devonian reef complexes|||||Conglomerate and sandstone.|30-JUL-15
28360|Behn Conglomerate|69165|6|Mentioned|500k_geologyp08_lut.csv|Famennian|Frasnian|||||||
28360|Behn Conglomerate|70126|5|Briefly described|Map legend|Famennian|Frasnian|Canning Basin.|||||Siliciclastic cobble to boulder conglomerate, minor sandstone and interbedded limestone; platform to basin level conglomerates associated with carbonate reef complexes.|
28360|Behn Conglomerate|70154|4|Described|100k_geologyp_lut.csv|Famennian|Frasnian||359-383 Ma||||Siliciclastic cobble to boulder conglomerate, minor sandstone and interbedded limestone;platform to basin level conglomerates associated with carbonate reef complexes.|
28360|Behn Conglomerate|71267|4|Described|GEOL_LUT_CSV files|Famennian|Frasnian|Of Lennard Shelf, Canning Basin. Events: Meda Transpression (323-310 Ma); Red Bluffs Extension (372.2-360 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma); Pillara Movement (Alice Springs Orogeny phase 2) (390-360 Ma); Van Emmerick Extension (382.7-372.2 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 100k_geologyp_lut.csv.|382.7-358.9 Ma (biostrat, inferrred)||||Siliciclastic cobble to boulder conglomerate, minor sandstone and interbedded limestone; Frasnian and Famennian platform to basin level conglomerates associated with carbonate reef complexes|
28074|Bell Rock gabbro|61339|6|Mentioned|Schematic section|||Informal name.||||||
28074|Bell Rock gabbro|69153|6|Mentioned|GA_geochron.csv|||Granophyre, Bell Rock Intrusion, Western Musgrave Block. Data migrated from OZCHRON1. Original comment: 'These zircons are from a granophyric pegmatite in the Bell Rock gabbro. The zircons are large, euhedral and simply zoned with high-U contents (~4000 ppm). The 26 data points define a single population concordant U-Pb age that dates igneous emplacement.'|||||Granophyric leucogranite|
23372|Bellary Formation|23570|5|Briefly described|p231 Appendix 1|||Of Fortescue Group.   Overlain by Mount Roe Basalt.   Maximum thickness: 400m. Geological Province: Pilbara Craton||||||
23372|Bellary Formation|23575|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Overlying unit Mount Roe Basalt. Geological Province Hamersley Basin.||||||07-NOV-08
23372|Bellary Formation|23612|5|Briefly described|p840|||Of Fortescue Group. Geological Province: Hamersley Basin.||||||
23372|Bellary Formation|24544|5|Briefly described|p57 Fig.43|Archean|Archean|Of Fortescue Group. Overlain by Mount Roe Basalt. Conglomerate. Geological Province: Hamersley Basin.||||||07-NOV-08
23372|Bellary Formation|42471|4|Described|p4|||Rocks previously assigned to Hardey Formation (1967) and basement succession (1985).||||||26-JUL-07
23372|Bellary Formation|42472|5|Briefly described|Map legend|Archean||||||||07-NOV-08
23372|Bellary Formation|42686|5|Briefly described|map legend|Archean||||||||07-NOV-08
23372|Bellary Formation|42704|5|Briefly described|Plate 2E|Archean||Combined with mount Roe Basalt in this map legend.||||||07-NOV-08
23372|Bellary Formation|42744|4|Described|p3|||||||||
23372|Bellary Formation|42785|5|Briefly described|Fig.3 P264|||||||||
23372|Bellary Formation|43119|4|Described|p5|||Of the Fortescue Group.||||||16-JAN-07
23372|Bellary Formation|60706|5|Briefly described|p625 Fig.3, p637 Fig.9|Archean|Archean|Of the Fortescue Group. Geological Province: Hamersley Basin.||||||07-NOV-08
23372|Bellary Formation|61259|5|Briefly described|p403|Archean|Archean|Geological Province: Pilbara Craton. See also p404 Fig. 1.||||||07-NOV-08
23372|Bellary Formation|63420|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group (Mount Bruce Supergroup). Overlies Lalla Rookh Sandstone in places; overlain by Mount Roe Basalt. Geol. Province: Marble Bar Sub-basin/Hamersley Basin. Coarse-grained to pebbly sandstone, minor pebble conglomerate; thickly bedded.||||||07-NOV-08
23372|Bellary Formation|64384|5|Briefly described|p29 Tb. 5|Archean|Archean|Of the Fortescue Group. Overlain by Mount Roe Basalt. Geological province: southern Hamersley Basin. Mudstone, siltstone, and sandstone; conglomerate, basalt, volcanic breccia and tuff.||||||07-FEB-11
23372|Bellary Formation|64580|4|Described|map legend||Neoarchean|Of Fortescue Group. Siliciclastic sedimentary rocks and basaltic volcanic rocks.||||||09-DEC-08
23372|Bellary Formation|64621|5|Briefly described|Map legend|Archean|Archean|Of Fortescue Group. Conglomerate, pebbly sandstone and sandstone; dominantly chert and quartz clasts; locally silicified. Shale and siltstone with brown weathering. Sandstone, pebbly sandstone + minor conglomerate.||||||07-NOV-08
23372|Bellary Formation|64724|6|Mentioned|p42 Fig. 3|Neoarchean|Neoarchean|||||||02-APR-12
23372|Bellary Formation|64936|5|Briefly described|map legend|Archean|Archean|Of Fortescue Group, Mount Bruce Supergroup. Under Mount Roe Basalt; unconformable over Lalla Rookh Sandstone. Conglomerate and sandstone. Geol. Prov: Hamersley Basin, Pilbara Craton.||||||
23372|Bellary Formation|66108|5|Briefly described|Map legend|Neoarchean|Neoarchean|Unit in Fortescue Group. Siliciclastic sedimentary rocks and basaltic volcanic rocks.||||||
23372|Bellary Formation|66217|4|Described|p5, p6 Table 1, p44 Fig.19, p45, p51.|Archean|Archean|Fortescue Basin, Pilbara Craton. Up to 556 m thick. The sedimentary rocks were deposited in braided fluviatile and lacustrine settings during tectonic instability, as evidenced by silicified coarse angular breccias.|<2830 and >2772 Ma.|Basal unit in Fortescue Group.||Unconformably overlies Lalla Rookh Sandstone. Is overlain by Mount Roe Basalt.|Dominantly clastic sedimentary rocks including conglomerate and sandstone, and subordinate mafic volcanic and volcaniclastic rocks.|12-DEC-12
23372|Bellary Formation|67130|5|Briefly described|p3 fig 2, p45|||||Fortescue Group||Intruded by Black Range Dolerite Suite, overlain by Mount Roe Basalt|Sandstone and siltstone.|
23372|Bellary Formation|67201|4|Described|p28-29|||In northern Pilbara Craton, Fortescue Basin.||Basal unit in Fortescue Group||Unconformably overlies irregular paleosurface composed of Whundo Group, Cleaverville Formation, and Whim Creek Group. Is overlain by Mount Roe Basalt.|Sedimentary.|22-NOV-16
23372|Bellary Formation|68035|5|Briefly described|p291, p292 Fig 6|Neoarchean|Neoarchean|Fortescue Basin. ?clastic units up to several hundred metres thick, and possibly also basaltic units up to 2 km thick.||Near base of Fortescue Group.||Underlies the Mount Roe Basalt in places. Intruded by Black Range Dolerite Suite. Overlies by unnamed basalt.|sandstone, siltstone.|
23372|Bellary Formation|68280|6|Mentioned|p5, p42|||||Fortescue Group|||Sandstone and siltstone.|13-JAN-23
23372|Bellary Formation|68281|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.||Of the Fortescue Group.|||Pebble to cobble conglomerate and coarse-grained to pebbly sandstone; dominantly chert and quartz clasts; locally silicified; thickly bedded.|23-SEP-13
23372|Bellary Formation|68283|5|Briefly described|Map Legend|Archean|Archean|Marble Bar Sub-basin, Fortescue Basin.||Of the Fortescue Group.|||Coarse-grained to pebbly sandstone; minor pebble conglomerate; thickly bedded.|23-SEP-13
23372|Bellary Formation|69028|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.||Of the Fortescue Group.|||Siliciclastic sedimentary and basaltic volcanic rocks; metamorphosed.|06-MAY-14
23372|Bellary Formation|69080|5|Briefly described|p687|Neoarchean|Neoarchean|||Basal unit in Fortescue Group.||Is overlain by Mount Roe Basalt.||
23372|Bellary Formation|69166|5|Briefly described|500k_geologyp08_lut.csv|Neoarchean|Neoarchean|||Fortescue Group|||Siliciclastic sedimentary rocks and basaltic volcanic rocks.|
23372|Bellary Formation|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Fortescue Group|||Pebble to cobble conglomerate,coarse grained to pebbly sandstone, and sandstone with dominantly chert and quartz clasts; locally silicified.|
23372|Bellary Formation|69185|4|Described|GEOL_LUT_CSV files||Neoarchean|Geological Province: Pilbara Craton. Of South Pilbara Sub-basin, Hamersley Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.||Unit of Fortescue Group.|||Siliciclastic sedimentary rocks and basaltic volcanic rocks|
23372|Bellary Formation|69301|6|Mentioned|p18 Fig.7|||Pilbara Craton. Fortescue Basin. South Pilbara Sub-basin, Sequence 1.||||||
23372|Bellary Formation|69590|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Of Marble Bar Sub-basin, South Pilbara Sub-basin, Fortescue Basin. Events: Capricorn Orogeny; Edmundian Orogeny; Ophthalmian Orogeny; Pilbara Craton breakup. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|2780-2775 Ma (inferred)|Unit of Fortescue Group.|||Conglomerate, pebbly sandstone, and sandstone; dominantly chert and quartz clasts; locally silicified; shale and siltstone.|
23372|Bellary Formation|70775|6|Mentioned|p71|||||Fortescue Group||||
23372|Bellary Formation|70795|6|Mentioned|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean||2775-2772 Ma|Fortescue Group|||Basaltic volcanic and siliciclastic sedimentary rocks; metamorphosed.|
23372|Bellary Formation|71169|5|Briefly described|p64|Neoarchean|Neoarchean||c. 2775 Ma|Fortescue Group||||
23372|Bellary Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||sandstone, conglomerate, shale pelite|
23372|Bellary Formation|71808|5|Briefly described|p7, p104, p149|||Pilbara Craton. Restricted to the core of the Bellary Dome near Paraburdoo and is not recognised elsewhere.||Fortescue Group|||Deltaic sediments and basalt.|
23372|Bellary Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Marble Bar Sub-basin; South Pilbara Sub-basin. Fortescue Basin.||Fortescue Group, sequence 1|||Siliciclastic sedimentary and basaltic volcanic rocks; metamorphosed.|
23372|Bellary Formation|72712|5|Briefly described|p8, p10 Fig.6.|Neoarchean|Neoarchean|Unconformably overlies unnamed granite-greenstone strata. Not recognised in Hardey Syncline area.|c 2775 Ma.|Base of Fortescue Group.||Underlies Mount Roe Basalt.||
23372|Bellary Formation|73538|6|Mentioned|p4|||||Fortescue Group||Overlain by Mount Roe Basalt Formation.|Mudstone/siltstone.|
29480|Bellevue Limestone Member|63454|4|Described|p76|Late Pleistocene|Late Pleistocene|Lower to middle part of Kooallup Limestone. Fossiliferous marine limestones+beach calcarenite; includes white to cream, shelly/bioturb.calcarenite, laminated x-laminated shelly calcarenite/coquina, lam.to x-lam. beach calcarenite. See also Bellevue Member||||||
77578|Beloceras Bed, Lower|66127|6|Mentioned|p422, p433 Fig.2.2.|Frasnian|Frasnian|||Unit in Virgin Hills Formation.||||
72567|Beloceras Bed, Upper|62735|6|Mentioned|p982|Frasnian|Frasnian|Informally named horizon within the Virgin Hills Formation. A transgressive marker bed with abundant trilobites. In the McWhae Ridge area. Geol. Prov: Canning Basin.||||||04-OCT-06
72567|Beloceras Bed, Upper|66127|6|Mentioned|p422.|Frasnian|Frasnian|||Unit in Virgin Hills Formation.||||
23374|Benalla Formation|13194|4|Described|p386 Tb. 4-16|Norian|Carnian|Type Section: North Hibernia 1 well (2553-3631m). Up to 1100m thick open-marine shelf deposits.||Sahul Group||Coeval with Challis Formation and Nome Formation.|Carbonate; minor shale and sandstone.|
23374|Benalla Formation|13222|6|Mentioned|p229 Fig.2.|||||Unit in Sahul Group.||||
23374|Benalla Formation|41532|2|Defined|p304|Middle Triassic||WA Definition. Same unit as Benalla Formation, NT.||||||08-NOV-06
23374|Benalla Formation|41716|5|Briefly described|p334|||||||||
23374|Benalla Formation|42442|2|Defined|p23|Norian|Carnian|NT Definition. Same unit as Benalla Formation, WA .||||||24-JUL-06
23374|Benalla Formation|69452|5|Briefly described|p36:15|Triassic|Triassic|Bonaparte Basin.||Sahul Group.||||12-JUL-16
23374|Benalla Formation|70061|6|Mentioned|Regional geology Fig.7|Norian|Norian|||Sahul Group.||||12-JUL-16
23377|Bent Tree Basalt|22534|4|Described|p8, Fig.4 p7|||of Grants Patch Group. See also p15||||||
23377|Bent Tree Basalt|22596|6|Mentioned|Fig.9 p419|||||||||
23377|Bent Tree Basalt|23808|6|Mentioned|p7|||||||||
23377|Bent Tree Basalt|23926|6|Mentioned|p22 Fig. 10|||Geological Province: Yilgarn Craton.||||||
23377|Bent Tree Basalt|42156|6|Mentioned|Fig.1 p373|||||||||26-FEB-16
23377|Bent Tree Basalt|42221|6|Mentioned|Table 1 P6|||||||||
23377|Bent Tree Basalt|42382|5|Briefly described|p19|||||||||
23377|Bent Tree Basalt|42436|6|Mentioned|p75|||||||||
23377|Bent Tree Basalt|42696|6|Mentioned|Plate 1B|||||||||
23377|Bent Tree Basalt|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
23377|Bent Tree Basalt|42870|5|Briefly described|Table 1, P67|||||||||
23377|Bent Tree Basalt|42989|5|Briefly described|Table 1,Fig.2|||||||||
23377|Bent Tree Basalt|43074|5|Briefly described|p9,Fig.6|||||||||
23377|Bent Tree Basalt|43101|5|Briefly described|Table 1.|||of Grants Patch Group||||||
23377|Bent Tree Basalt|43102|5|Briefly described|p8|||||||||
23377|Bent Tree Basalt|43162|6|Mentioned|5|||||||||
23377|Bent Tree Basalt|43496|6|Mentioned|6|||||||||
23377|Bent Tree Basalt|50551|5|Briefly described|p1092 Fig.3||Archean|Alternating pillowed, massive doleritic and coarse-grained layers. In Eastern Goldfields Province.||||||07-NOV-08
23377|Bent Tree Basalt|60076|5|Briefly described|p12 Tb. 2|||Massive pillowed lavas, including mafic sills.  Max. thickness: <3000m.  Geological Province: Ora Banda domain.||||||
23377|Bent Tree Basalt|60514|5|Briefly described|p61, p64, p64 Fig. 5|Archean|Archean|Of the Grants Patch Group. Contact with the Victorious Basalt is planar and intensely sheared. High-Mg basalt and dolerite. Geological Province: Yilgarn Craton.||||||07-FEB-11
23377|Bent Tree Basalt|60627|5|Briefly described|p61, p65 Tb.1|||High-Mg basalt and dolerite. Of Grants Patch Group.||||||
23377|Bent Tree Basalt|63981|6|Mentioned|p93 Fig.3, |Archean|Archean|Ora Banda Domain. Kambalda Sequence. |||||Tholeiitic and high MgO basalt.|
23377|Bent Tree Basalt|65204|5|Briefly described|pg6 Tbl.1, p12, p13|Neoarchean||Tholeiitic basalt; intruded by Mount Pleasant and Mount Ellis Sills; overlies Big Dick Basalt.||||||11-JUN-15
23377|Bent Tree Basalt|65834|5|Briefly described|p7, 13, 37-39|||Mount Pleasant district, Ora Banda Domain, Kalgoorlie Terrane.||Grants Patch Group.||Overlies Coppermine Shale.|Flow basalt.|
23377|Bent Tree Basalt|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2726 - 2680 Ma (inferred).|Kalgoorlie Group|||Tholeiitic basalt; pillowed to massive; metamorphosed.|
23377|Bent Tree Basalt|70326|5|Briefly described|p360-362|Neoarchean|Neoarchean|Geological province: Ora Banda region, Ora Banda Domain, Kalgoorlie Terrane, Yilgarn Craton. ||||Overlain by Vcictorious Basalt. Underlain by Bif Dick Basalt. Intruded by Mount Pleasant Sill.||
23377|Bent Tree Basalt|71166|5|Briefly described|p9 fig 3.4a|||Hosts gold mineralisation. See also p20 fig 3.13, p26, p27 fig 3.20.||||Underlies the Victorious Basalt.|Phaneritic basalt.|
23377|Bent Tree Basalt|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2726-2680 Ma (inferred)|Unit of Vetters Subgroup.|||Tholeiitic basalt; pillowed to massive; metamorphosed; Pyroxene spinifex-textured basalt; locally variolitic and/or pillowed; metamorphosed.|
23377|Bent Tree Basalt|72814|5|Briefly described|p201, Fig. 3, p202 Fig. 4, p204, p205|||East of Zuleika Shear, Ora Banda Domain.|||||Mafic pillowed basalt flows.|
23377|Bent Tree Basalt|73391|5|Briefly described|p51, 53, 75, 78, 80, 88, 194, 202, 244|||See also p254, 267, 279, 310, 324, 330-331, 343-344, 363, Appendices. Ora Banda Domain, Eastern Goldfields Province. This is described as the lower of two tholeiitic mafic flows (separated by a thin discontinuous horizon of carbonaceous shale) of the Upper Basalt. 2000m thick.||Grants Patch Group; Upper Basalt.||Overlies Siberia Komatiite, Mount Pleasant Sill, Big Dick Basalt, Coppermine Shale. Is overlain by Victorious Basalt.|Massive/pillowed basalt, high Mg, tholeiitic. Intercalated basalt flow units with thin, interflow, carbonaceous shale beds,|
23377|Bent Tree Basalt|73596|6|Mentioned|p1160|||Appears as Devon Consol/Bent Tree Basalt.||||||
38576|Bertibubba Supersuite|23781|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Formerly "Wooramel suite" and "Bertibubba suite".||||||07-NOV-08
38576|Bertibubba Supersuite|24544|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|Granite. Age: 1965-1945 Ma. Formerly the "Wooramel Suite".||||||07-NOV-08
38576|Bertibubba Supersuite|50216|5|Briefly described|p203|Paleoproterozoic|Paleoproterozoic|Biotite monzogranite. Age: 1965-1945 Ma. Intrudes the Yarlarweelor Gneiss Complex, Camel Hill Metamorphics and parts of the Narryer Terrane and Glenburgh Terrane.||||||07-NOV-08
38576|Bertibubba Supersuite|50218|5|Briefly described|p239|Orosirian|Orosirian|Formerly the Wooramel suite of Ochipinti et al (1999b). Biotite monzogranite. Age: 1965-1945Ma. Locally intruded and deformed the Yarlarweelor Gneiss Complex. Geological Province: Errabiddy Shear Zone. See also Figs. 2 and 3, p240-41.||||||07-FEB-11
38576|Bertibubba Supersuite|50219|5|Briefly described|p260 Fig. 2|Orosirian|Orosirian|Formerly the Wooramel suite of Sheppard et al (1999).  Age: 1965-1945Ma.  Geological Province: Gascoyne Complex, Errabiddy Shear Zone..||||||29-SEP-11
38576|Bertibubba Supersuite|50220|5|Briefly described|p280, p281 Fig.1|Orosirian|Orosirian|Formerly the Wooramel suite. Granite. Age: 1960 Ma. See also p292 Tb.2.||||||
38576|Bertibubba Supersuite|50226|6|Mentioned|p418|||Granite plutons.||||||
38576|Bertibubba Supersuite|63866|5|Briefly described|p152, p155-p158, p161, p168, p177|||Yilgarn Craton and Glenburgh Terrane. Granitic dykes which intrude the Nardoo Granite may be related to the Bertibubba Supersuite. Ages derived from Nelson, 1998; Kinny et al, 2004.|1970 +/- 15 Ma and 1956 +/-9 Ma|||||
38576|Bertibubba Supersuite|64161|6|Mentioned|p590|Orosirian|Orosirian|Granite-dominated. Intruded during the 2005-1960 Ma Glenburgh Orogeny, Gascoyne Complex||||||
38576|Bertibubba Supersuite|64580|4|Described|map legend||Paleoproterozoic|Granitic rocks.||||||15-DEC-08
38576|Bertibubba Supersuite|64728|6|Mentioned|p107.|||Southern Gascoyne Complex. Probable source of detrital zircons aged 2400-1850 Ma found in Ashburton Formation and Pooranoo Metamorphics.||||||
38576|Bertibubba Supersuite|65545|6|Mentioned|Bedrock geology|||Gascoyne Province.Shown in error? Doesn't seem to appear on map face.||||||
38576|Bertibubba Supersuite|65549|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Gascoyne Province. Includes Yamagee Granite, the only named unit shown. Age of c. 1960 Ma given.||||||
38576|Bertibubba Supersuite|65830|5|Briefly described|p24|Orosirian|Orosirian|Granites of the Bertibubba Supersuite intruded into the southern margin of the Glenburgh Terrane, Errabiddy Shear Zone and northern margin of the Yilgarn Craton at 1965-1945 Ma.|~ 1965-1945 Ma|||||
38576|Bertibubba Supersuite|66299|4|Described|p4 Fig.2, pp104-110.|Paleoproterozoic|Paleoproterozoic|The first element common to Glenburgh Terrane and Yilgarn Craton; interpreted as having stitched these terranes together.|1965-1955 Ma and dykes c.1945 Ma.||Includes Yamagee Granite.|Intrudes Yarlarweelor Gneiss Complex, Camel Hills Metamorphics and Dalgaringa Supersuite.|Equigranular and porphyritic, biotite metamonzogranite; lesser dykes of leucocratic, biotite tonalite, and granodiorite.|
38576|Bertibubba Supersuite|66887|4|Described|p3 Fig.2, p5 Fig.4, p6|Paleoproterozoic|Paleoproterozoic|Southern Gascoyne Province. First magmatic element common to the northern margin of Yilgarn Craton, Yarlarweelor Gneiss Complex, Earabiddy Shear Zone, and Glenburgh Terrane.|1965-1945 Ma|||Intrudes Yarlarweelor Gneiss Complex.|Granite.|
38576|Bertibubba Supersuite|66950|5|Briefly described|p7, p9 Fig.8, p10 Fig.9, p13, p14, p21|Orosirian|Orosirian||c. 1965-1945 Ma||||Comprises biotite-muscovite granites.|
38576|Bertibubba Supersuite|67371|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|c.1945 Ma.||||Fine-grained, massive, leucocratic tonalite and granodiorite.|
38576|Bertibubba Supersuite|67843|4|Described|p2 Fig.1, p5, p38.|Paleoproterozoic|Paleoproterozoic|Widely spread intrusions, from the Glenburgh Terrane to the Yilgarn Craton. Deformed granites have crystallisation ages of 1965-1955 Ma, whereas an undeformed dyke has a crystallisation age of 1945 +/- 14 Ma; thus deformation has ended by then.|1965-1945 Ma.|||Intrudes Yarlarweelor Gneiss Complex and Nardoo Granite.|Includes plutons of tectonically foliated, variably porphyritic, biotite-bearing, and leucocratic monzogranite, and undeformed dykes of coarse-grained leucocratic tonalite and granodiorite.|
38576|Bertibubba Supersuite|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic||||||granitic rocks|
38576|Bertibubba Supersuite|69003|5|Briefly described|p4, p10|||Capricorn Orogen. Intruded the N margin of the Yilgarn Craton, the Errabiddy Shear Zone, and the S margin of the Glenburgh Terrane, during the 2005-1950 Ma Glenburgh Orogeny.|1965-1945 Ma.||||Granite stocks and dykes.|
38576|Bertibubba Supersuite|69028|5|Briefly described|Map Legend|Orosirian|Orosirian|Gascoyne Province.|1965-1945 Ma||||Granite and metagranitic rocks.|06-MAY-14
38576|Bertibubba Supersuite|69080|5|Briefly described|p684, p689, p696|Orosirian|Orosirian|Gascoyne Province. Formed during the 1965-1950 Ma collision of Yilgarn Craton with the amalgamated Pilbara Craton-Glenburgh Terrane (the Glenburgh Orogeny).|1965-1945 Ma.||||Stocks and dykes of granite and metagranitic rocks.|
38576|Bertibubba Supersuite|69166|5|Briefly described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic||||Includes Yamagee Granite||Fine-grained, massive, leucocratic tonalite and granodiorite.|
38576|Bertibubba Supersuite|69387|5|Briefly described|p3, p6, p9, p11-13, p21-22, p27-28|Orosirian|Orosirian|Gascoyne Province. This is the first common element across the Yilgarn Craton and combined Pilbara-Glenburgh Terrane. SG and magnetic susceptibility values given. Gravity and magnetic modelling.|1965-1945 Ma.||||Granitic stocks and dykes.|
38576|Bertibubba Supersuite|69583|5|Briefly described|p130, p132, p159; Plates 2, 3|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Associated with the Glenburgh Orogeny.|c.1965-1945 Ma.||||Granitic and metagranitic stocks and dykes.|
38576|Bertibubba Supersuite|69596|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|Yilgarn Craton.||||||
38576|Bertibubba Supersuite|70795|5|Briefly described|2_5m_interpgeop15_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_geologyl_lut.csv, West Australian Craton|1961-1945 Ma||||Granite and metagranitic rocks. Fine grained, massive, leucocratic tonalite and granodiorite.|
38576|Bertibubba Supersuite|70796|4|Described|2_5m_interpgeop15_lut.csv|Paleoproterozoic|Paleoproterozoic|Of the Capricorn Orogen, Gascoyne Province. Affected by the following events:  Mulka Tectonic Event (570  570 Ma); Edmundian Orogeny D3e/M3e (995  954 Ma); Edmundian Orogeny (1026  954 Ma); Edmundian Orogeny D1e/M1e (1026  995 Ma); Edmundian Orogeny D2e/M2e (1026  995 Ma); Mutherbukin Tectonic Event (1321  1171 Ma); Mangaroon. See also 500k_interpgeop14_lut.csv.|1961 +/ 6 Ma to 1945 +/ 14 Ma (isotopic)||||Granite and metagranitic rocks|
38576|Bertibubba Supersuite|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|Southern Gascoyne Province.||||Intrudes the Camel Hills Metamorphics.||
38576|Bertibubba Supersuite|71000|6|Mentioned|p64-65|Paleoproterozoic|Paleoproterozoic|Intrudes the Erabiddy Shear Zone.|1965-1945 Ma.||||Granitic stocks and dykes.|
38576|Bertibubba Supersuite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||gneiss, granite|
38576|Bertibubba Supersuite|71269|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Gascoyne Province; Capricorn Orogen, West Australian Craton. Events: Mulka Tectonic Event (570-570 Ma); Edmundian Orogeny D3e/M3e (995-954 Ma); Edmundian Orogeny (1026-954 Ma); Edmundian Orogeny D1e/M1e (1026-995 Ma); Edmundian Orogeny D2e/M2e (1026-995 Ma); Mutherbukin Tectonic Event (1321-1171 Ma); Mangaroon??.  See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv.|1961+\-6, 1845+\-14 Ma||||Granite and metagranitic rocks|
38576|Bertibubba Supersuite|71484|6|Mentioned|p125|||Geological province:  Of Padbury Basin [?].|||||Granite and metagranitic rocks.|30-AUG-19
38576|Bertibubba Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Gascoyne Province, Capricorn Orogen.||Max age 1961+/-6 Ma, min age 1945 +/-14 Ma.|||Granite and metagranitic rocks.|
38576|Bertibubba Supersuite|72259|6|Mentioned|p3, App. Tb.B|Orosirian|Orosirian||ca. 2005-1945 Ma||||Includes granitic gneiss and monzogranite.|
38576|Bertibubba Supersuite|72705|6|Mentioned|p3|||Capricorn Orogeny. Post-(Glenburgh Orogeny)orogenic.|1965 -1945 Ma.|||||
38576|Bertibubba Supersuite|73102|5|Briefly described|p3|||Gascoyne Province.|||||Granite and metagranitic rocks.|
38576|Bertibubba Supersuite|73214|5|Briefly described|p974 Fig.1|Palaeoproterozoic|Palaeoproterozoic|Affected by the 2005-1950 Ma Glenburgh Orogeny.||||||
38576|Bertibubba Supersuite|73442|5|Briefly described|p3|||Gascoyne Province.|||||Granite and metagranitic rocks.|
39730|Beryl pegmatite group|24193|4|Described|p887|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
24715|Bessie Creek Sandstone|22538|6|Mentioned|Fig3 P708|||||||||
24715|Bessie Creek Sandstone|22600|4|Described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24715|Bessie Creek Sandstone|23216|5|Briefly described|Table1p8,33-4|||||||||
24715|Bessie Creek Sandstone|23404|5|Briefly described|p645|||||||||
24715|Bessie Creek Sandstone|23776|5|Briefly described|p709|||Of Roper Group.||||||
24715|Bessie Creek Sandstone|23937|2|Defined|p74 App. 1|Calymmian|Calymmian|Now assigned to the redefined Maiwok Subgroup (Roper Group). Conformably overlain by Velkerri Formation; overlies the Corcoran Formation.  Max. thickness: 56m, 217m in type section on BAUHINIA DOWNS.  Geological Province: McArthur Basin. See also p42.||||||13-APR-05
24715|Bessie Creek Sandstone|24048|4|Described|p71|Mesoproterozoic|Paleoproterozoic|Of the Roper Group.  Geological Province: McArthur Basin.||||||07-NOV-08
24715|Bessie Creek Sandstone|24049|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Quartz arenite: buff to red-brown, fine to coarse-grained, thin to medium-bedded; common thin to medium quartz granule conglomerate beds, planar and trough cross-beds, ripples. Geol. Prov: McArthur Basin.||||||13-OCT-05
24715|Bessie Creek Sandstone|24050|4|Described|p50, p8 Tb. 2|Mesoproterozoic|Mesoproterozoic|Medium-grained quartz sandstone.  Of the Roper Group.  Overlies Corcoran Formation.  Max. thickness: >10m.||||||24-JUL-06
24715|Bessie Creek Sandstone|24051|5|Briefly described|Map Legend|Calymmian|Calymmian|Of Roper Group. Geological Province: McArthur Basin.||||||
24715|Bessie Creek Sandstone|24303|5|Briefly described|p34, p61 Appendix|||Of the Roper Group. Geological Province: McArthur Basin. Correlates with the Jangirulu Formation. See also p24 Tb. 4.||||||
24715|Bessie Creek Sandstone|32660|5|Briefly described|Table 4|||||||||
24715|Bessie Creek Sandstone|37568|6|Mentioned|Fig.6|||||||||
24715|Bessie Creek Sandstone|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24715|Bessie Creek Sandstone|40691|6|Mentioned|p64|||||||||
24715|Bessie Creek Sandstone|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24715|Bessie Creek Sandstone|41268|6|Mentioned|p292|||||||||
24715|Bessie Creek Sandstone|41531|6|Mentioned|p167|||||||||
24715|Bessie Creek Sandstone|42385|6|Mentioned|p30|||||||||
24715|Bessie Creek Sandstone|42395|6|Mentioned|Fig.26 P86|||||||||
24715|Bessie Creek Sandstone|42597|5|Briefly described|Map Legend|Adelaidean||||||||
24715|Bessie Creek Sandstone|42639|4|Described|p44, Table 7 p39|||||||||
24715|Bessie Creek Sandstone|42812|3|Fully described|p53, Table 5|||Of Roper Group.||||||24-JUL-06
24715|Bessie Creek Sandstone|42846|5|Briefly described|Fig.1 p502|||Of Roper Group. Geological Province: McArthur Basin.||||||09-MAY-05
24715|Bessie Creek Sandstone|43010|4|Described|Table 30.|||Of Roper Group||||||24-JUL-06
24715|Bessie Creek Sandstone|43036|6|Mentioned|Fig.5|||of Roper Group||||||
24715|Bessie Creek Sandstone|43149|5|Briefly described|Map Legend||Mesoproterozoic|Of Roper Group. Of Calymmian age.||||||24-JUL-06
24715|Bessie Creek Sandstone|43645|5|Briefly described|p562|||||||||
24715|Bessie Creek Sandstone|43652|6|Mentioned|p386|||||||||
24715|Bessie Creek Sandstone|44112|6|Mentioned|Fig11p30|||||||||
24715|Bessie Creek Sandstone|44201|14|Not recorded|p.9|||||||||
24715|Bessie Creek Sandstone|44287|14|Not recorded|p.12,18, opp.11|||(E53-3).||||||
24715|Bessie Creek Sandstone|44288|14|Not recorded|map legend|||Quartz sandstone, Upper (?) Proterozoic.||||||
24715|Bessie Creek Sandstone|44299|4|Described|p.13|||SD/53-7,8. U (?) Proterozoic. Table 1.||||||
24715|Bessie Creek Sandstone|44300|14|Not recorded|map legend||Neoproterozoic|SD/53-7,8. U.Proterozoic, pt of Roper Gp.||||||
24715|Bessie Creek Sandstone|44332|14|Not recorded|p.8-9,12,opp.6,map|||(D53-14). Friable.||||||
24715|Bessie Creek Sandstone|44333|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
24715|Bessie Creek Sandstone|44400|2|Defined|p.9,Tb.1,opp.p.6,map|||Mt.Marubma Sheet. (D53-6).||||||
24715|Bessie Creek Sandstone|44401|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
24715|Bessie Creek Sandstone|44434|14|Not recorded|p.8, opp. p.6, map|||(D53-11,12).||||||
24715|Bessie Creek Sandstone|44435|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
24715|Bessie Creek Sandstone|44459|14|Not recorded|p.8, opp.p.6, map|||(E53-2). Formation of Roper Group.||||||
24715|Bessie Creek Sandstone|44460|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
24715|Bessie Creek Sandstone|44471|14|Not recorded|p.9,opp.p.7, map|||(D53-10). See also p.10,14, for more details.||||||
24715|Bessie Creek Sandstone|44472|5|Briefly described|map legend|||Of the Roper Group.  Massive white friable quartz sandstone.  Upper (?) Proterozoic.||||||02-DEC-04
24715|Bessie Creek Sandstone|44530|14|Not recorded|p.12,18,opp, 12|||(D53-15).||||||
24715|Bessie Creek Sandstone|44531|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
24715|Bessie Creek Sandstone|45022|14|Not recorded|p.78,81, TB11, PL28||Adelaidean|Of Roper Group||||||
24715|Bessie Creek Sandstone|45162|6|Mentioned|Fig.4|||||||||
24715|Bessie Creek Sandstone|46679|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
24715|Bessie Creek Sandstone|46861|6|Mentioned|Fig.2A|||||||||
24715|Bessie Creek Sandstone|60483|5|Briefly described|p7 Fig. 5|||Of the Roper Group. Geological Province: McArthur Basin.||||||05-OCT-07
24715|Bessie Creek Sandstone|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Roper Group. Overlain by Maiwok Subgroup, underlain by Corcoran Formation.||||||
24715|Bessie Creek Sandstone|61250|5|Briefly described|p43|Mesoproterozoic|Mesoproterozoic|Contains rich petroleum systems. Geological Province: Beetaloo Sub-basin.||||||27-MAY-06
24715|Bessie Creek Sandstone|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Maiwok Subgroup. Quartz sandstone: fine to medium and locally coarse grained, tough cross-stratifycation, ripple marks.||||||29-SEP-05
24715|Bessie Creek Sandstone|61403|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Quartz arenite: buff to red-brown, fine to coarse-grained, thin to medium-bedded; common thin to medium quartz granule conglomerate be ds, planar and trough cross-beds, ripples. Geol. Prov: McArthur Basin.||||||
24715|Bessie Creek Sandstone|61566|5|Briefly described|p622|Proterozoic|Proterozoic|Of the Roper Group. Morphologically prominent mature quartzite and sandstone deposits. Geological Province: McArthur Basin.||||||26-APR-06
24715|Bessie Creek Sandstone|62376|5|Briefly described|p38|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Geological Province: Beetaloo Sub-Basin.||||||09-FEB-10
24715|Bessie Creek Sandstone|62759|5|Briefly described|p1|Mesoproterozoic|Mesoproterozoic|Geological Province: Beetaloo Sub-basin. Contains oil reservoirs.||||||05-FEB-08
24715|Bessie Creek Sandstone|64784|4|Described|p2 Fig.2, p3 Fig.3, p4-5, p7, p10 |Proterozoic|Proterozoic|Beetaloo Basin. A significant reservoir in the Basin.||Unit in Roper Group.||Overlies Corcoran Formation. Is overlain by Velkerri Formation.|Generally fine- to very fine-grained with occasional medium grain size, and is light to medium to dark gray in colour. Over 400m thick.|
24715|Bessie Creek Sandstone|64816|5|Briefly described|p1-6, p8-21             |Proterozoic|Proterozoic|A potential reservoir unit for Velkerri Formation oil. Pacific Oil and Gas wells encountered good oil shows at the top of this unit. Chemistry of oil inclusions detailed.||Unit in Roper Group.|||Fine- to medium-grained, well sorted, extremely well-cemented quartz arenite with low visible porosity.|
24715|Bessie Creek Sandstone|64817|6|Mentioned|p353 Fig.4 |||||Of the Roper Group.||||
24715|Bessie Creek Sandstone|64975|6|Mentioned|p162 Fig.6.|Mesoproterozoic|Mesoproterozoic|||Unit in Roper Group.||||
24715|Bessie Creek Sandstone|65228|6|Mentioned|Fig.02.|||||Unit in Roper Group.||Overlies Corcoran Formation. Is overlain by Velkerri Formation.||
24715|Bessie Creek Sandstone|65236|5|Briefly described|p2, p3 Fig. 3, p4 Fig. 4|Mesoproterozoic|Mesoproterozoic|Overlain by Velkerri Formation. Geological province: Beetaloo Sub-basin.||||||04-JUN-09
24715|Bessie Creek Sandstone|65342|6|Mentioned|p9, p12. |||Daly Basin. Max. thickness at least 61 m.||||||
24715|Bessie Creek Sandstone|69018|4|Described|p449-451, 454, 456, 457, 459-461|Calymmian|Calymmian|Part of marine succession. Estimated maximum burial 2.5 km, corresponding to ~75 degrees C. Contains water/gas/oil inclusions as well as bitumen.||Of Roper Group.||Intruded by 1280-1220 Ma dolerite sill at top, in places. Is overlain by Velkerri Formation.|Fine- to medium-grained, well-sorted and well-cemented quartz arenite|
24715|Bessie Creek Sandstone|69430|4|Described|p15:3, 27, 29-31, 62-63|Calymmian|Calymmian|McArthur Basin. c.20-56m thick; up to 400m in Beetaloo Sub-basin. Coastal tidal platform sediments. Caps mesas and buttes. Forms the spectacular "Ruined City" of joint-bounded, karstically weathered towers up to 50m high. Fair to good conventional hydrocarbon reservoirs occur, and has potential for unconventional reservoirs (basin-centred gas), in structural and diagenetic traps. The overlying Velkerri Formation may have been both source rock and seal.||Maiwok Subgroup.||Disconformably overlies Corcoran Formation. Is overlain conformably by Velkerri Formation.|Fine to medium, locally coarse and granule-rich quartz sandstone; mainly thinly to medium bedded and trough cross-stratified.|12-JUL-16
24715|Bessie Creek Sandstone|69673|5|Briefly described|p20, p32, p36, p40, p44, p46|||Northwestern and Southern McArthur Basin. Conventional reservoir potential. Up to 442m thick.||Maiwok Subgroup||Conformably overlain by Velkerri Formation, Disconformably overlies Corcoran Formation|Sandstone and mudstone with pore filling bitumen in places.|
24715|Bessie Creek Sandstone|70734|5|Briefly described|p14, 16, 17|||McArthur Basin. Tidal platform sandstone.||Of Maiwok Subgroup.||Overlain by Velkerri Formation. Overlies Corcoran Formation.||
24715|Bessie Creek Sandstone|70822|5|Briefly described|p102 fig 1 (A), p104|Mesoproterozoic|Mesoproterozoic|||Roper Group||Overlies Corcoran Formation; overlain by Velkerri Formation.|Sandstone.|
24715|Bessie Creek Sandstone|70897|6|Mentioned|Fig.1.7.6,9|||Appears simply as Bessie in Fig.1.7.6. McArthur Basin.||||||
24715|Bessie Creek Sandstone|70968|2|Defined|v, p39, p42, p47-48, p50-51, p55-59, p61|Ectasian|Ectasian|See also p65, p124, p126-129, p131, p137, p140, p143. Sweet and Abbott in Abbott et al. (2001) after Dunn (1963). Included in Maiwok Subgroup by Abbott et al. (2001). Named after Bessie Creek. The type section is NW of Beetle Springs at 605000mE 8143700mN (base) to 604800mE 8143500mN in BAUHINIA DOWNS sheet. Widely distributed in McArthur Basin. Forms spectacular parakarstic landforms, eg the Lost City (Limmen National Park) of joint-bounded towers up to 50m high. Resistant unit. Lithology described and illustrated in some detail. Has potential as conventional and unconventional oil/gas reservoir. Thickness from 25m to 367m; 217m in the type section. Deposition in a high-energy tide-dominated shoreline to shallow shelf setting. Detrital zircon diagram and discussion.||Maiwok Subgroup.||Conformably (locally disconformably) overlies Corcoran Formation. Is overlain conformably by Velkerri Formation. Is intruded by Derim Derim Dolerite sills. Correlated with Jangirulu Formation.|White when fresh, mainly fine- to medium-grained clean quartz sandstone, friable when weathered; mudstone partings and thin, locally abundant intraclast-rich intervals; Liesegang banding common.|
24715|Bessie Creek Sandstone|71059|4|Described|p3, p10|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 10-417m thick. Coastal tidal platform deposits. Estimated shale/tight gas/shale oil and condensate resources detailed.||Maiwok Subgroup.||Conformably to disconformably overlies Corcoran Formation. Is overlain conformably by Velkerri Formation.|Fine to medium, locally coarse and granule-rich quartz sandstone.|
24715|Bessie Creek Sandstone|71488|4|Described|p140-p153|Ectasian|Ectasian|Beetaloo Sub-basin. Ages are interpreted as maximum depositional ages. Deposited in a high-energy tidal shoreline to shallow marine shelf setting.|1386 +/- 13 Ma and 1417 +/- 29 Ma|Maiwok Subgroup||Overlies the Corcoran Formation. Conformably overlain by the Velkerri Formation. Overlain by the Moroak Sandstone.|Highly mature quartz sandstones.|01-MAY-18
24715|Bessie Creek Sandstone|71779|5|Briefly described|iii, p2, p6-p9, p12 fig 9, p24-p25|||Urapunga, Beetaloo Sub-basin and Bauhinia Downs Regions, McArthur Basin. See also figs on p10, 11.||Of Maiwok Subgroup.||Conformably overlain by the Kalala Member (Velkerri Formation).|Cross-bedded fine sandstone is typical.|24-SEP-18
24715|Bessie Creek Sandstone|71893|4|Described|p2-p5, p8, p28-p31|Calymmian|Calymmian|McArthur Basin. A maximum depositional age of 1575 +/- 19 Ma and a youngest individual age of 1385 +/- 116 Ma are provided. Deposited in a high-energy, tide-dominated shoreline to shallow marine shelf setting. A maximum age is derived from the underlying Showell Member dated at 1493 +/- 4 Ma and a minimum age of 1361 +/- 21 Ma is derived from Re-Os of the Wyworrie Member of the overlying Velkerri Formation. Zircon description, LAICPMS U-Pb and Hf analysis, results and interpretation are provided.||Maiwok Subgroup||Conformably (or gradationally) overlies the Corcoran Formation.|Thinly- to medium-bedded, cross-bedded, locally coarse-grained and granule-rich quartz sandstone.|
24715|Bessie Creek Sandstone|72381|4|Described|p771-779|Mesoproterozoic|Mesoproterozoic|Of Beetaloo Sub-basin, McArthur Basin. Deposited in a high-energy tide dominated shoreline to shallow shelf setting (Pietsch et al. 1991; Abbott et al. 2001; Munson 2016). Deposition is coeval with post-orogenic Mount Isa Province exhumations (c. 1460 and 1390 Ma), nothern Gawler Craton magmatism and high-grade metamorphism c. 1540 (Morrissey et al., 2018) and eastern Gawler Craton exhumation (c. 1420 Ma; Foster and Ehlers 1998). Maximum depositional age constrained by youngest detrital zircon age of 1386+\-13 Ma (youngest near-concordant detrital zircon; Yang et al., 2018). Combined U-Pb and Hf isotopic analysis indicate a mixed provenance from the north (e.g. Pine Creek Orogen, Halls Creek Orogen) and east or SE (e.g. Mount Isa region and adjacent terranes).|c. 1.4 Ga|Unit of Mailwok Subgroup.||Lowermost unit of Maiwok Subgroup. Overlain by Velkerri Formation. Underlain by Corcoran Formation. Intruded by Derim Derim Dolerite.|Highly mature quartz arenite.|04-OCT-19
24715|Bessie Creek Sandstone|72526|5|Briefly described|p8 Fig.1.3.|Ectasian|Calymmian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin and northern part of the Batten Fault Zone.||Maiwok Subgroup||Overlies Corcoran Formation and underlies Velkerri Formation.||
24715|Bessie Creek Sandstone|72718|6|Mentioned|p7, p10|||Southern McArthur Basin. Urapunga Fault Zone, southwestern McArthur Basin, and Batten Fault Zone (north). Notable seismic reflector (coherent impedance boundaries) used for calibration of well-logs and are continuous over long distances.||Maiwok Subgroup, Roper Group||Underlain by Corcoran Formation. Overlain by Velkerri Formation.||
24715|Bessie Creek Sandstone|72912|5|Briefly described|p5 Fig.3.|Mesoproterozoic|Mesoproterozoic|Located in the Urapunga Fault Zone, Beetaloo Sub-basin and the northern part of the Batten Fault Zone in the Southern McArthur Basin.||Maiwok Subgroup||Overlies Corcoran Formation and underlies Velkerri Formation.||
24715|Bessie Creek Sandstone|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Southern McArthur Basin, Roper Superbasin.||Maiwok Subgroup, Roper Group||Underlain by Corcoran Formation. Overlain by Velkerri Formation.||
24715|Bessie Creek Sandstone|73242|5|Briefly described|p39|||||Maiwok Subgroup, Roper Group||Underlain by Corcoran Formation. Overlain by Kalala Member, Velkerri Formation. Intruded by Derim Derim Dolerite.|Includes tidal Sandstone.|
24715|Bessie Creek Sandstone|73412|5|Briefly described|p4, 8|||Southern McArthur Basin.||Maiwok Subgroup.||Overlies Corcoran Formation. Is overlain by Velkerri Formation.||
29421|Beta Island Member|42959|5|Briefly described|p63|||of Roysalt Formation||||||
29421|Beta Island Member|43761|4|Described|p420-421|||||||||
29421|Beta Island Member|43838|6|Mentioned|p4||Tertiary|Within Redmine Group||||||12-JUL-16
29421|Beta Island Member|65194|5|Briefly described|p137|||Unit in Roysalt Formation. Gypsum-bearing lunette dunes. Likely formed in the Quaternary.||||||
29218|Betty Formation|7433|5|Briefly described|p33.|Early Permian|Late Carboniferous|||Unit in lower Grant Group.|||Fine to coarse, sparsely fossiliferous clastics.|
29218|Betty Formation|22718|6|Mentioned|P5|||||||||
29218|Betty Formation|22738|5|Briefly described|12|Early Permian|Early Permian|Parent Grant Group. Overlying unit Winifred Formation.||||||24-NOV-08
29218|Betty Formation|22741|5|Briefly described|P25, Table3 P14||Sakmarian|||||||
29218|Betty Formation|22753|6|Mentioned|p535|||Obsolete subdivision of Grant Group||||||
29218|Betty Formation|22765|6|Mentioned|P9||Permian|||||||
29218|Betty Formation|22767|5|Briefly described|Table3 P16, P21|Early Permian|Late Carboniferous|||||||
29218|Betty Formation|22776|4|Described|Table.3|Early Permian|Late Carboniferous|Fossil assemblage includes palynomorphs.||||||
29218|Betty Formation|22801|6|Mentioned|P11||Permian|||||||
29218|Betty Formation|23212|5|Briefly described|Table.1 p7||Early Permian|Of Grant Group.||||||24-NOV-08
29218|Betty Formation|23765|5|Briefly described|Map Legend|Permian|Carboniferous|||||||23-DEC-09
29218|Betty Formation|23766|4|Described|p14 Tb. 2|Late Carboniferous|Late Carboniferous|Comprised of sandstone and minor conglomerate. Parent: Grant Group. Thickness: 801m.  See also p17.||||||24-NOV-08
29218|Betty Formation|24246|5|Briefly described|p9|Permian|Carboniferous|Geological Province: Canning Basin.||||||
29218|Betty Formation|36224|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Of the Grant Group.  Sandstone, very fine to coarse; minor conglomerate.||||||01-FEB-05
29218|Betty Formation|36225|6|Mentioned|Map legend|Early Permian|Late Carboniferous|Late Carboniferous to Early Permian||||||
29218|Betty Formation|36634|6|Mentioned|Map legend|Early Permian|Late Carboniferous|Late Carboniferous to Early Permian||||||
29218|Betty Formation|37914|5|Briefly described|p450|||See also P449.||||||
29218|Betty Formation|41215|6|Mentioned|p280|||See also P281||||||
29218|Betty Formation|41315|6|Mentioned|p135|||||||||
29218|Betty Formation|41839|4|Described|p26|||||||||
29218|Betty Formation|42547|3|Fully described|p97|||Part of Grant Group.||||||
29218|Betty Formation|42613|2|Defined|P 4|Sakmarian|Late Carboniferous|Of Grant Group.||||||24-NOV-08
29218|Betty Formation|42734|5|Briefly described|map legend|Carboniferous||||||||
29218|Betty Formation|43015|5|Briefly described|Table 1,p319|||Of Grant Group.||||||24-NOV-08
29218|Betty Formation|43563|6|Mentioned|Fig.9,p15||Early Permian|||||||
29218|Betty Formation|43816|6|Mentioned|p88|||||||||
29218|Betty Formation|43818|6|Mentioned|Table 2,p42|||||||||
29218|Betty Formation|44143|4|Described|p.436 Table 4-19; p.446|Permian|Carboniferous|Unit in Grant Group. Up to 1720m thick, sandstone and some conglomerate; ablation diamictites; shallow-water glacial environment. Is overlain conformably by Winifred Formation. Type section between 1058-1675m in Lake Betty 1 (MOUNT BANNERMAN 19deg 34' 10" S, 126deg 19' 52" E).||||||22-NOV-17
29218|Betty Formation|45158|4|Described|p22|||||||||
29218|Betty Formation|49644|5|Briefly described|Table|||||||||
29218|Betty Formation|64580|6|Mentioned|map legend|||Of Grant Group.||||||15-DEC-08
29218|Betty Formation|64630|5|Briefly described|p31 Fig.2, p35|||Superseded name? Of Grant Group, in Fitzroy Trough area. Replaced by Reeves Formation.||||||
29218|Betty Formation|64643|5|Briefly described|p8|Sakmarian|Asselian|Of Grant Group in Fitzroy Trough. Does not crop out.||||||
29218|Betty Formation|64971|5|Briefly described|p686, p685 Fig. 2|Early Permian|Late Carboniferous|Of Crowe and Towner (1976). Of Grant Group.||||||09-FEB-10
29218|Betty Formation|64974|5|Briefly described|p148 Fig. 6|Asselian|Asselian|Of Grant Group. Geological Province: Canning Basin.||||||24-JUN-09
29218|Betty Formation|64981|5|Briefly described|p669 Fig.3.|Asselian|Late Carboniferous|Oil was recovered from a fluvial-channel sand within this unit; recovery in the Sundown oil field had declined to a barely economic level by the time of this article.||Unit in Grant Group.||Unconformably overlies Anderson Formation. Is overlain by Winifred Formation.|Non-marine, coarse-grained clastic rocks with erratics of glacial origin.|
29218|Betty Formation|64982|5|Briefly described|pp699-700.|||||Unit in Grant Group.|||Sandstone and conglomerate.|
29218|Betty Formation|66949|4|Described|p9-10, p13, p16, p28, p54 Appx.2|Asselian|Sakmarian|See also p58 Appx.3, p60-65 Appx.4; p72,78-80,84-86,88,90,92,04 Appx.5; Plates 2-12. Subsurface only; unconformably overlies pre-Permian rocks. Type section in Late Betty 1 detailed. Up to ?1714m thick (in Grant Range 1); shallow water glacial deposits. Identified with Reeves Formation (Apak and Backhouse, 1989, 1999) and thus obsolete (reasons are discussed); equivalent to Paterson Formation. A 1-2 m thick shale bed forms a sealing horizon in the Boundary field on the Lennard Shelf. Available core and Formation picks detailed.||Unit in Grant Group.||Appears to be equivalent to Hoya and Reeves Formations.|Sandstone and conglomerate/diamictite, minor siltstone. Dolerite intersected in Minjin 1 and Perindi 1 wells.|30-OCT-15
29218|Betty Formation|68007|4|Described|p2, p9-10, p12, Plates 1, 2|Permian|Permian|Southern Canning Basin. c.379m thick in Patience 2 well. Composite well log. Overlies Reeves Formation in Frankenstein 1, Kidson 1. Unconformably overlies ?Clapp Ridge Formation in Contention Heights 1, Wilson Cliffs 1, Patience 1 & 2.||Grant Group.||Overlies Reeves Formation (probably conformably) or Clapp Ridge Formation unconformably. Is overlain by Winifred Formation. Equivalent to Hoya Formation.|Dominantly light grey sandstone, sometimes calcareous, fining upwards; interbeds of light to dark grey claystone and siltstone, the latter locally calcareous and often micaceous.|20-FEB-20
29218|Betty Formation|68656|6|Mentioned|GEOL_LUT_CSV/500k_geologyp08_lut|||||Grant Group||||
29218|Betty Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Cisuralian|Pennsylvanian|||||||
29218|Betty Formation|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Grant Group.||||
29218|Betty Formation|69693|5|Briefly described|p3-5, 9-10|Permian|Carboniferous|Lennard Shelf, Canning Basin. Serpukhovian to Sakmarian. See also references to Betty formation (p2,4).||||Unconformably overlies Anderson Formation. Is overlain by Winifred Formation. Equivalent to Hoya Formation.|Mixed sandstone and diamictite rich unit.|
29218|Betty Formation|72496|4|Described|p217-231|Sakmarian|Asselian|Canning Basin, Lennard Shelf, Fitzroy Trough. Has slightly higher and more variable gamma ray readings in comparison to the underlying Reeves Formation. Ranges in thickness from 82 to 417.5m; thickness is fairly constant in the Fitzroy Trough. Deposited in a glacial deltaic to fluvial environment.||Grant Group||Equivalent to the Hoya Formation. Unconformably overlies the Reeves Formation. Overlain by the Winifred Formation.|Fining upwards sequence of sandstone, sand and mud rich diamictite and mudstones.|18-MAR-20
29218|Betty Formation|72497|5|Briefly described|p4.|Carboniferous|Carboniferous|After Crowe and Towner, 1976. Part equivalent to informal lower Grant Group of Redfern and Millward, 1994.||||Shown as underlying Winifred Formation.||
29218|Betty Formation|72499|4|Described|p54 Fig.48, p93-94.|Cisuralian|Cisuralian|Associated facies recorded on well logs Sundown 1 and Sundown 3/3H (Lennard Shelf), The Sisters 1 and Scarpia 1 (Fitzroy Trough), Frome Rocks 2 (Jurgurra Terrace), Dampier Downs 1 and Roebuck Bay 1 (Broome Platform) and Perindi 1 (Pender Terrace).||Grant Group||Overlies Reeves Formation and underlies Winifred Formation.|Includes diamictites, turbidites and mudstone, with fluvial-shallow marine sandstone, cross-bedded sandstone.|
29218|Betty Formation|73117|4|Described|p: 22-23, 25, 110, ~122-125, 136, 139|||Of Crowe and Towner (1976). [Written as 'Betty Formation' and 'Betty' ... Formations]. Part of the 'three ladies' naming scheme proposed as a subdivision of the Grant Group. Authors consider this an informal unit. This scheme for constituents of the Grant Group has been widely applied but is considered flawed by the authors because of spatially isolated type sections.||Grant Group||||
27337|Beverley Springs Member|30533|6|Mentioned|p15|||Possibly equivalent of King Leopold Sandstone||||||
27337|Beverley Springs Member|30896|4|Described|p18|||||||||
27337|Beverley Springs Member|31226|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
27337|Beverley Springs Member|32728|5|Briefly described|Table 7|||||||||
27337|Beverley Springs Member|36888|4|Described|p213|||||||||
27337|Beverley Springs Member|48931|4|Described|p60|||||||||
27337|Beverley Springs Member|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Mount House Sub-basin, Louisa Basin.||Walsh Tillite|||Poorly sorted, pebbly quartz sandstone.|30-JUL-15
27337|Beverley Springs Member|69634|4|Described|250k_geologyp_lut.csv|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Mount House Sub-basin, Louisa Basin, Centralian Superbasin. Events: King Leopold Orogeny D1/M1; King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1. See 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|635-541 Ma (Inferred)|Unit of Walsh Tillite.|||Poorly sorted, pebbly quartz sandstone|
27337|Beverley Springs Member|69660|5|Briefly described|Map legend|Cryogenian|Cryogenian|Louisa Basin, North Australian Craton.||Unit in Walsh Tillite.|||Poorly sorted, pebbly quartz sandstone.|
27337|Beverley Springs Member|70154|5|Briefly described|250k_geologyp_lut.csv|Cryogenian|Cryogenian|See also 250k_interpgeop_lut.csv.|635-650 Ma|Walsh Tillite|||Poorly sorted, pebbly quartz sandstone|
27337|Beverley Springs Member|71267|4|Described|GEOL_LUT_CSV files|Cryogenian|Cryogenian|Geological province: King Leopold Orogen. Of Mount House Sub-basin, Louisa Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma). See 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|650-635 Ma (inferred)|Unit of Walsh Tillite.|||Poorly sorted, pebbly quartz sandstone|
81586|Beverly Hills Dolerite|72057|6|Mentioned|p242|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton.||Unit of Cave Rocks Dolerite.||||
74796|Biddenew Formation|66110|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Mount James Subgroup. Age shown as 1758-1677 Ma. Feldspathic metasandstone and minor feldspathic pebbly metasandstone; medium- to coarse-grained; locally ripple marked and cross-bedded.||||||
74796|Biddenew Formation|66299|4|Described|p51, p56, pp215-232.|Paleoproterozoic|Paleoproterozoic|Intruded by units of Durlacher Supersuite.|1758 +/- 18 Ma to 1677 +/- 5 Ma.|Unit in Mount James Subgroup.||Is overlain by Spring Camp Formation, Mount Augustus Sandstone and Edmund Group. Unconformably overlies Halfway Gneiss.|Fluvial succession of metaconglomerate, feldspathic metasandstone, phyllite or slate and psammitic schist.|
74796|Biddenew Formation|66579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Unit in Mount James Subgroup.|||Feldspathic metasandstone and minor feldspathic pebbly metasandstone; medium- to coarse-grained; locally ripple-marked and cross-bedded.|
74796|Biddenew Formation|66950|6|Mentioned|p12|||||Of the Mount James Subgroup.||||
74796|Biddenew Formation|67371|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|1758 - 1677 Ma.|Unit in Mount James Subgroup.|||Feldspathic metasandstone and minor feldspathic pebbly metasandstone; medium- to coarse-grained; locally ripple-marked and cross-bedded; minor phyllite and slate, cobble and boulder metaconglomerate.|
74796|Biddenew Formation|67373|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|1758 - 1677 Ma.|Unit in Mount James Subgroup.|||Coarse-grained, granule and pebble-rich feldspathic metasandstone; minor quartz-muscovite schist.|
74796|Biddenew Formation|68521|5|Briefly described|Map Legend|Statherian|Statherian|4 unnamed sub-units are mapped separately.||Of the Mount James Subgroup.|||Undivided: feldspathic metasandstone and minor feldspathic pebbly metasandstone; medium- to coarse-grained; locally ripple marked and cross-bedded. Also mapped are granule and pebbly feldspathic metasandstone; phyllite; schist; metaconglomerate.|
74796|Biddenew Formation|68522|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|5 facies are mapped separately.||Of the Mount James Subgroup.|||Feldspathic metasandstone and minor feldspathic pebbly metasandstone, medium- to coarse-grained, locally ripple marked and cross-bedded; coarse-grained feldspathic metasandstone; phyllite and slate; schist; cobble and boulder metaconglomerate.|
74796|Biddenew Formation|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Age derived from quartz metasandstone sample (183255.1.pdf)|1749 Ma +/- 9 Ma(SHRIMP)|Mount James Subgroup||Conformably overlain by Spring Camp Formation|Interbedded slate and metasandstone. Phyllite and slate, biotite-quartz-muscovite schist and quartz-muscovite-biotite schist. Coarse grained pebbly feldspathic metasandstone, quartz-muscovite schist. Cobble and boulder metaconglomerate.|
74796|Biddenew Formation|70127|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Some facies are mapped separately.|1741-1682 Ma.|Pooranoo Metamorphics.|||Undivided: feldspathic metasandstone and minor feldspathic pebbly metasandstone, medium- to coarse-grained, locally ripple-marked and cross-bedded. Cobble and boulder metaconglomerate, strongly foliated; phyllite and slate.|
74796|Biddenew Formation|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 183255.1.pdf|1758-1683 Ma|Mount James Subgroup||Conformably overlain by Spring Camp Formation|Feldspathic metasandstone and minor feldspathic pebbly metasandstone, slate, quartz metasandstone, phyllite, biotite-quartz-muscovite schist. Coarse grained, granule and pebbly feldspathic metasandstone.|
74796|Biddenew Formation|71273|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.||Pooranoo Metamorphics.|||Feldspathic metasandstone and minor feldspathic pebbly metasandstone; medium- to coarse-grained; locally ripple-marked and cross-bedded. (Separately mapped) phyllite and slate; granule and pebbly feldspathic metasandstone.|
74825|Big Bell Suite|64891|5|Briefly described|p34 Fig. 1, p42, p50-51 Tb. 1|Archean|Archean|Of the Austin Downs Supersuite. Includes Crossroads Granodiorite, and Batchelor and Tough Go Monzogranites. Age: 2716-2694Ma. Geological province: Murchison Domain. Foliated tonalitic to monzogranitic rocks. Referred to as a Granite Suite in Fig. 2.||||||07-FEB-11
74825|Big Bell Suite|66195|5|Briefly described|p599 Fig.2|Neoarchean||In the Austin Downs Supersuite. Granitic.||||||02-MAY-16
74825|Big Bell Suite|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Mapped as six separate units, only one of which - Crossroads Granodiorite - is named.|age range at least 2724-2702 Ma|Unit in Austin Downs Supersuite.|Includes Crossroads Granodiorite and five separately-mapped but un-named units.||Biotite metamonzogranite, foliated; K-feldspar megacrystic biotite metamonzogranite; metagranodiorite; biotite metagranodiorite, strongly foliated with pegmatite veins; pegmatite-layered metamonzogranite gneiss.|18-NOV-13
74825|Big Bell Suite|67129|5|Briefly described|p18 Fig.19, p19 Fig.20|Archean|Archean|Murchison Domain, Youanmi Terrane.||Austin Downs Supersuite|Crossroads, Tough Go Monzogranites.||Granites, sheared and metamorphosed tholeiitic pillow basalts, mafic schists.|06-SEP-17
74825|Big Bell Suite|68108|5|Briefly described|p628, p649|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. Appears as Supersuite in p649|ca. 2716-2694 Ma||||Late-volcanic granites.|
74825|Big Bell Suite|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane||Austin Downs Supersuite|Includes Crossroads Granodiorite and 7 unnamed units.||Metagranite; commonly foliated; includes granodiorite to monzogranite|
74825|Big Bell Suite|68698|5|Briefly described|p3-6, p10-11, p14-17, p19, p27-28|Neoarchean|Neoarchean|Geochemistry is discussed briefly. REE plots.|c.2720-2690 Ma.|Austin Downs Supersuite.||||
74825|Big Bell Suite|69014|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. 6 unnamed facies, mapped separately.|2735-2690 Ma|Of the Austin Downs Supersuite.|||Metamonzogranites: biotite, locally strongly sheared; foliated leucocratic; foliated muscovite; strongly foliated, locally quartz porphyritic; K-feldspar megacrystic biotite; medium-grained mesocratic with gneiss.|01-MAY-14
74825|Big Bell Suite|69583|4|Described|p49, p51-53, p99, p105, p108; Plate 2|Neoarchean|Neoarchean|Murchison Domain. Comprises the felsic intrusives of the Austin Downs Supersuite. Described as late-volcanic granites. Age also given as 2716-2694 Ma. Seismic interpretation.|c.2724-2690 Ma.|Austin Downs Supersuite.|Crossroads Granodiorite.|Is sheared against Windimurra Igneous Complex.|Tonalitic to monzogranitic rocks. Metagranite, metamonzogranite, K-feldspar-megacrystic biotite metamonzogranite, K-feldspar porphyritic monzogranite; equigranular monzogranite to syenogranite; all foliated.|
74825|Big Bell Suite|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean|||Austin Downs Supersuite|Crossroads Granodiorite|||
74825|Big Bell Suite|69586|5|Briefly described|p22, p31 Fig.33|Neoarchean|Neoarchean|Murchison Domain.||Austin Downs Supersuite.|Crossroads Granodiorite.|||
74825|Big Bell Suite|69627|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton||Austin Downs Supersuite|Crossroads Granodiorite||Metamonzogranite, locally quartz pophyritic, strongly foliated; monzogranite to syenogranite (leucocratic), undeformed local magmatic foliation; Crossroads Granodiorite (biotite metagranodiorite).|
74825|Big Bell Suite|69628|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. The four facies are mapped separately.||Austin Downs Supersuite|||Muscovite metamonzogranite, foliated; metamonzogranite, locally quartz porphyritic, strongly foliated; K-feldspar megacrystic biotite metamonzogranite, strongly foliated; granitic gneiss with deformed pegmatite veins, foliated and lineated.|
74825|Big Bell Suite|70020|5|Briefly described|p118|Neoarchean|Neoarchean|Geological province: Yilgarn Craton.||||Overlain by Tuckanarra Suite.||
74825|Big Bell Suite|70030|5|Briefly described|p191-192|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton.|2716-2694 Ma|Unit of Austin Downs Supersuite.|Includes Crossroads Monzogranite and Tough Go Monzogranite.||Granites.|17-JUL-19
74825|Big Bell Suite|70139|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton. The five facies are mapped separately.|c.2724-c.2702 Ma.|Austin Downs Supersuite.|||Metamonzogranites. Interleaved with schistose metabasalt; medium-grained, mesocratic, foliated, and gneiss; K-feldspar megacrystic, strongly foliated; locally quartz porphyritic, strongly foliated; biotite, generally leucocratic, commonly foliated.|
74825|Big Bell Suite|70153|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean||2735 - 2690 Ma (inferred).|Austin Downs Supersuite|||Metagranite; commonly foliated; includes granodiorite to monzogranite.|
74825|Big Bell Suite|70156|4|Described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Youanmi Terrane events (3200-2600 Ma).|2735-2690 Ma (inferred)|Unit of Austin Downs Supersuite.|||Metagranite; commonly foliated; includes granodiorite to monzogranite|
74825|Big Bell Suite|70226|5|Briefly described|Map legend.|Neoarchean|Neoarchean| Murchison Domain, Youanmi Terrane, Yilgarn Carton.|c. 2710 Ma (Fletcher and McNaughton, 2002).|Austin Downs Supersuite.|||Metagranodiorite; monzogranite dykes in greenstones; metamorphosed.|16-DEC-15
74825|Big Bell Suite|70418|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Fifteen facies are mapped separately.||Austin Downs Supersuite.|||Monzogranites, syenogranites, granitic gneiss, metagranodiorite.|
74825|Big Bell Suite|70419|5|Briefly described|p3, p10, p13-15, p17, p25, p26 Fig.10|Neoarchean|Neoarchean|Has a sheared contact with the Windimurra Igneous Complex and truncates many igneous layers.|c.2700 Ma.||||Metamonzogranites.|
74825|Big Bell Suite|70420|6|Mentioned|p9 Fig.6|Archean|Archean|||||||
74825|Big Bell Suite|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton. Five facies are mapped separately.|c.2735-2690 Ma.|Austin Downs Supersuite.|||Metagranite to metagranodiorite with rafts of metagabbro; monzogranite to syenogranite, undeformed; fine-grained monzogranite dykes in greenstones; schistose granodiorite; moderately foliated metagranodiorite.|
74825|Big Bell Suite|70794|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Youanmi Terrane, Yilgarn Craton. Also 2_5m_interpgeop15_lut.csv.|2735-2690  Ma|Of Austin Downs Supersuite.|||Metagranite; commonly foliated; includes granodiorite to monzogranite.|
74825|Big Bell Suite|70796|4|Described|2_5m_interpgeop15_lut.csv|Neoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. Affected by the Yilgarn Craton granite magmatism (3010  2600 Ma); Youanmi Terrane events (3131  2600 Ma). See also 100k_geologyl_lut.csv, 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 155501.1.pdf,155502.1.pdf,155503.1.pdf, 155504.1.pdf, 155505.1.pdf, 155507.1.pdf,155511.1.pdf,185922.1.pdf, 185923.1.pdf, Austin100_2442_stratig.pdf, Badja100_2240_stratig.pdf, Cue100_2443_stratig.pdf, MountMagnet100_2441_stratig.pdf, Nowthanna100_2643_stratig.pdf, Reedy100_2543_stratig.pdf, Wynyangoo100_2542_stratig.pdf. Numerous additional lithologies are discussed.|2735 to 2690 Ma (inferred)|Austin Downs Supersuite|Includes the Crossroads Granodiorite.|Coeval with the Yalgowra Suite.|Metagranite; commonly foliated; includes granodiorite to monzogranite. Granitic gneiss, biotite metamonzogranite, leucocratic monzogranite. Metagranodiorite,|
74825|Big Bell Suite|70830|5|Briefly described|p8-p10, p33, p40, p58|Neoarchean|Neoarchean|Murchison Domain. |c. 2716-2694 Ma|Austin Downs Supersuite|||Granites.|
74825|Big Bell Suite|71159|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton. The two facies are mapped separately.||Austin Downs Supersuite.|||Medium-grained, locally porphyritic, schistose to gneissic metamonzogranite; schistose metagranodiorite, locally strongly sheared.|
74825|Big Bell Suite|71168|5|Briefly described|p7|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c. 2730-2690 Ma|Austin Downs Supersuite|||Granitic rocks.|
74825|Big Bell Suite|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Zircon dating yields ages of  2690+\-5 Ma (GSWA155501), 2868+\-4 Ma (GSWA 155502), 2702+\-4 Ma (GSWA155503), 2706+\-4 Ma (GSWA155504), 2732+\-6 Ma (GSWA155507), 2715+\-5 Ma (GSWA155510) and 2728+\-9 Ma (GSWA155511) intepreted as magmatic crystallisation ages of the dyke; weighted mean zircon age of 2716+\-12 Ma (GSWA155505) interpreted as maximum age of dyke intrusion. Sample GSWA 199700 (biotite monzogranite) yielded a weighted mean 207Pb/206Pb date of 2700+\-4 Ma, interpreted as the magmatic crystallization age of the monzogranite. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv.|2735-2690 Ma (inferred)|Unit of Austin Downs Supersuite.|Includes Crossroads Granodiorite.|Coeval with Glen Group and Yalgowra Suite.|Granitic gneiss with rafts of migmatitic tonalite, monzogranite to syenogranite, metamonzogranite; foliated leucocratic, muscovite, gneissic, k-spar megacrystic, metatonalite, metagranodiorite.|
74825|Big Bell Suite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma); Youanmi Terrane events (3131 - 2600 Ma). See 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|2735-2690 Ma (inferred)|Unit of Austin Downs Supersuite.|||Metagranite; commonly foliated; includes granodiorite to monzogranite|
74825|Big Bell Suite|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|2690-2675 Ma.|Austin Downs Supersuite.|||Medium-grained metamonzogranite; locally porphyritic; schistose to gneissic.|
74825|Big Bell Suite|71272|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Six facies are mapped separately.|2735-2690 Ma.|Austin Downs Supersuite.|||K-feldspar-phyric monzogranite; equigranular monzogranite to syenogranite; metamonzogranite to metatonalite; K-feldspar-megacrystic biotite metamonzogranite; metagranodiorite, locally schlieric and gneissic; granitic gneiss.|
74825|Big Bell Suite|71311|6|Mentioned|p795|||Mount Magnet greenstone belt area.||||||
74825|Big Bell Suite|71809|5|Briefly described|map legend|Archean|Archean|Yilgarn Craton, Youanmi Terrane||Of Austin Downs Supersuite.|||Includes K-feldspar porphyritic monzogranite; common magmatic foliation. Equigranular monzogranite to syenogranite; common magmatic foliation and schlieren layering.|
74825|Big Bell Suite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Youanmi Terrane.||Austin Downs Supersuite|Includes Crossroads Granodiorite and 4 unnamed units.||Metagranite; includes granodiorite to monzogranite. Muscovite metamonzogranite. K-feldspar megacrystic biotite metamonzogranite. Equigranular monzogranite to syenogranite. K-feldspar porphyritic monzogranite. All commonly foliated.|
74825|Big Bell Suite|72389|5|Briefly described|Map Legend|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Gabanintha 1:100k map sheet 2644. Includes numerous unnamed constituents.|2735-2686 Ma||||Metagranite; commonly foliated; includes granodiorite to monzogranite.|28-AUG-20
74825|Big Bell Suite|73023|5|Briefly described|p3, 15|Neoarchaean|Neoarchaean||2735-2690 Ma.||||Large-scale syntectonic high-Ca granite plutons.|
74825|Big Bell Suite|73410|6|Mentioned|p2|||Youanmi Terrane.|2730-2690 Ma.|||||
74825|Big Bell Suite|73453|6|Mentioned|p2|||||||||
74825|Big Bell Suite|73596|6|Mentioned|p1168|Neoarchean|Neoarchean|Yilgarn Craton.|2730-2690 Ma.|||||
23383|Big Dick Basalt|22534|4|Described|p15, Fig.4 p7|||of Linger and Die Group||||||
23383|Big Dick Basalt|22596|6|Mentioned|Fig.9 p419|||||||||
23383|Big Dick Basalt|42221|6|Mentioned|Table 1 P143|||||||||
23383|Big Dick Basalt|42382|5|Briefly described|p20|||||||||
23383|Big Dick Basalt|42436|6|Mentioned|p75|||||||||
23383|Big Dick Basalt|42696|6|Mentioned|Plate 1B|||||||||
23383|Big Dick Basalt|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
23383|Big Dick Basalt|42870|5|Briefly described|Table 1, P67|||||||||
23383|Big Dick Basalt|42989|5|Briefly described|Table 1,Fig.2|||||||||
23383|Big Dick Basalt|43074|6|Mentioned|Fig.6.|||||||||
23383|Big Dick Basalt|43101|5|Briefly described|Table 1.|||of Linger and Die Group||||||
23383|Big Dick Basalt|43102|5|Briefly described|p8|||||||||
23383|Big Dick Basalt|43162|6|Mentioned|5|||||||||
23383|Big Dick Basalt|43496|6|Mentioned|6|||||||||
23383|Big Dick Basalt|50551|5|Briefly described|p1094 Fig.5||Archean|In Eastern Goldfields Province.||||||07-NOV-08
23383|Big Dick Basalt|60076|5|Briefly described|p12 Tb. 2|||Max. thickness: <500m.  Geological Province: Ora Banda domain.||||||
23383|Big Dick Basalt|60514|5|Briefly described|p65 Table 1.|Archean|Archean|Of the Linger and Die Group. Overlain by Grants Patch Group, underlain by Siberia Komatiite. Geological Province: Ora Banda Domain.||||||07-FEB-11
23383|Big Dick Basalt|60627|5|Briefly described|p65 Tb.1|||Of Linger and Die Group.||||||
23383|Big Dick Basalt|63981|6|Mentioned|p93 Fig.3, |Archean|Archean|Ora Banda Domain. Kambalda Sequence. |||||Komatiite and high MgO basalt.|
23383|Big Dick Basalt|65204|6|Mentioned|pg6 Tbl.1, p11, p13|Archean|Archean|Komatiitic basalt. Of Linger and Die Group. Overlies Siberia Komatiite; is overlain by Bent Tree Basalt.||||||
23383|Big Dick Basalt|65834|6|Mentioned|p7|||Ora Banda Domain, Kalgoorlie Terrane.||Linger and Die Group.||||
23383|Big Dick Basalt|70326|5|Briefly described|p360,362|Neoarchean|Neoarchean|Geological province: Ora Banda region, Ora Banda Domain, Kalgoorlie Terrane, Yilgarn Craton. ||||Overlain by Bent tree Basalt. Underlain by Siberia Komatiite.||
23383|Big Dick Basalt|71166|6|Mentioned|p9 fig 3.4a|||||||||
23383|Big Dick Basalt|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2726-2680 Ma (inferred)|Unit of Vetters Subgroup.|||Variolitic basalt;  pillowed to massive; metamorphosed; Komatiitic basalt; locally preserved relict pyroxene spinifex texture; metamorphosed|
23383|Big Dick Basalt|73391|5|Briefly described|p53, 194, 244, 279, Appendices.|||Ora Banda Domain, Kalgoorlie Terrane. 500m thick.||Linger and Die Group.||Overlies Siberia Komatiite. Is overlain by Bent Tree Basalt.|Ocellar high-Mg basalt, locally pillowed.|
23383|Big Dick Basalt|73596|6|Mentioned|p1160|||Appears as Big Dick Basalt/Tripod Hill Komatiite.||||||
80070|Big Red paragneiss|69595|5|Briefly described|p10 tbl 2, p15, p16 tbl 3, p18, p19, p32|Ectasian|Statherian|Informal name. Other ages provided. Eastern Nornalup Zone. Deposited in a moderate to low energy, intermediate to deep? marine. At least 50m thick. Misspelt as the Big Red para-gneiss on p16. Other significant age components are mentioned (see page 18). Significant portions of this unit are made up of c. 1800 Ma detritus. See also p35, p36, p37, p38. Analyses compared with Kybulup Schist.|1685 +/- 11 Ma -1326 +/- 6 Ma||||Migmatitic paragneiss|01-SEP-22
80070|Big Red paragneiss|70090|4|Described|p444,446-453,457-458|Statherian|Statherian|Geological province: Nornalup Zone, Albany-Fraser Orogen, West Australian Craton. Of Barren Basin, Depositional environment: Moderate to low energy, intermediate to deep marine? Thickness: >50m. Sedimentary protoliths deposited between 1710 Ma and 1650 Ma during Biranup Orogeny. Metamorphosed to amphibolite to granulite facies, during Zanthus Event. Maximum depositional age: c.1763 Ma. Minimum depositional age: contrained by c. 1326+\-6 Ma intrusive granitic gneiss. Comprises three major zircon age components: 1) ages >2700 Ma with an evolution array and 0.011 Lu/Hf ratio indicating recycled Archean crust distinct from Yilgarn Craton or a younger deep basement source from eastern part of Eastern Goldfields Superterrane; 2) c. 2600-2300 Ma, with two age sub-groupings and Hf isotopic compsition indicating a) reworking of crust similar to that of Southern Cross Domain (Yilgarn) and b) more radiogenic crust reworked at 2.5-2.4 Ga; and 3) between 1800 and 1700 Ma, overlapping in age and isotopic composition with Biranup Zone magmatic rocks.|||||Siltstone and mudstone?|
80070|Big Red paragneiss|70182|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|Deposition was coincident with the Biranup Orogeny.|Between 1710 Ma and 1650 Ma.|||||
74174|Big Spring Formation|64580|6|Mentioned|map legend|||Frasnian and Famennian conglomerates associated with Devonian reef complexes.||||||15-DEC-08
74174|Big Spring Formation|66127|4|Described|p143, Plates 2, 7.|Frasnian|Frasnian|Formerly Big Spring Member (of the Pillara Formation) of Read (1973b); amended to Big Spring Formation by Hocking and Playford (1998b). Named after Big Spring on Leopold Downs Station.||||Overlies Hooper Complex. Is overlain by / grades into Pillara Limestone.|Cyclic units (to 20 m thick) of coarse-grained arkosic sandstone, well-bedded to massive; locally calcareous, with massive siliciclastic conglomerate at the base; siltstone, shale and carbonates towards the top; fan-delta and alluvial-cone deposits.|
74174|Big Spring Formation|69099|5|Briefly described|500k_geologyp08_lut.csv|Famennian|Frasnian|Frasnian and Famennian conglomerates associated with Devonian reef complexes|||||Conglomerate and sandstone.|30-JUL-15
74174|Big Spring Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Famennian|Frasnian|||||||
79566|Big Tank Monzogranite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2726-2600 Ma (inferred)||||Biotite monzogranite; numerous pegmatitic dykes|
23384|Biggada Formation|6876|6|Mentioned|p100 Fig.5.|Jurassic|Jurassic|Equivalent units are shown on the diagram.||||||
23384|Biggada Formation|23379|4|Described|p160 Fig.2; p158,159,164,165,167,169,171|Callovian|Bathonian|Of Barrow Sub-basin, Carnarvon Basin.||||||01-SEP-08
23384|Biggada Formation|23726|5|Briefly described|p8 Fig 2c|Middle Jurassic|Middle Jurassic|Overlying unit Dupuy Formation. Underlying unit Athol Formation. Geological Province: Carnarvon Basin.||||||
23384|Biggada Formation|24246|5|Briefly described|p18, 19|Late Jurassic|Late Jurassic|Geological Province: Carnarvon Basin.||||||
23384|Biggada Formation|24390|5|Briefly described|p24 Table 6|||Geological Provine: Northern Carnarvon Basin.||||||
23384|Biggada Formation|40617|2|Defined|p8|Middle Jurassic|Early Jurassic|Early to Middle Jurassic E - M.||||||01-SEP-08
23384|Biggada Formation|41271|3|Fully described|p125|||Previously "Biggada Beds".||||||01-SEP-08
23384|Biggada Formation|41436|6|Mentioned|p45|||||||||
23384|Biggada Formation|41438|6|Mentioned|p107|||||||||
23384|Biggada Formation|41440|4|Described|p137|||||||||
23384|Biggada Formation|41732|6|Mentioned|p534|||||||||
23384|Biggada Formation|42116|5|Briefly described|Fig.1 P6|||||||||
23384|Biggada Formation|42615|1|Redefined|p34|Oxfordian middle|Oxfordian middle|Redefinition intended? - Age changed. Late Jurassic (middle Oxfordian)||||||
23384|Biggada Formation|43712|6|Mentioned|p11|||||||||
23384|Biggada Formation|43722|6|Mentioned|p10|||||||||
23384|Biggada Formation|43724|6|Mentioned|p29|||||||||
23384|Biggada Formation|50085|6|Mentioned|p24 Tb. 6|||Geological Province: Northern Carnarvon Basin.||||||
23384|Biggada Formation|62734|5|Briefly described|p1362 Fig. 2|Late Jurassic|Late Jurassic|Geological Province: Barrow Sub-basin.||||||01-SEP-08
23384|Biggada Formation|67200|5|Briefly described|p8 fig 6, |Jurassic|Jurassic|||||Overlies Athol Formation, overlain by Dupuy Formation|Sandstone and Siltstone.|
23384|Biggada Formation|68135|6|Mentioned|p51 fig 2|Oxfordian|Oxfordian|Northern Carnarvon Basin.||||||
23384|Biggada Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Northern Carnarvon Basin.||||||
23384|Biggada Formation|70066|5|Briefly described|Regional: Fig.6; p6, p16|Oxfordian|Oxfordian|Barrow Sub-basin, Northern Carnarvon Basin. Significant hydrocarbon reservoir: gas reserves estimated at 515 Bcf have yet to be developed.||||Overlies Calypso Formation. Is overlain by Dingo Claystone. Equivalent to Eliassen Formation.||
79825|Bight Basin Group|69632|5|Briefly described|p26|Cretaceous|Cretaceous||||Madura, Loongana Formations.|Is overlain by the Eucla Group.||
23385|Billabalong Basalt|42533|3|Fully described|p81|||Name reserved.||||||
23385|Billabalong Basalt|44149|5|Briefly described|p33 fig 2-29, p35 fig 2-30, p41|Archean|Archean|See also p44 Fig.2-46, p47. Of Murchison Province; western side of Twin Peaks greenstone belt. 2.5km thick sequence. Remnants of a shield volcano.||Mount Farmer Group|||Basal high-Mg basalt, then massive tholeiitic basalt with abundant gabbro and dolerite sills; pyroclastic tholeiites in top 1 km, interlayered (in upper 500 m) with felsic volcanics and scarce ferruginous chert, intensely deformed and intruded.|
23385|Billabalong Basalt|65268|6|Mentioned|p6 fig 4, p5 fig 3|||||Unit in Mount Farmer Group.|||Mainly tholeiitic basalt.|
42069|Billabong Complex|23809|5|Briefly described|p3 Fig. 1|||See also Billabong complex.||||||10-NOV-04
42069|Billabong Complex|61056|6|Mentioned|p778 Fig. 1a||Archean|Term used in a structural context. Age: 2514+/-3Ma.||||||07-NOV-08
42069|Billabong Complex|62580|5|Briefly described|p8|Archean|Archean|Includes othogneiss. Age: 2514+/-3Ma.||||||07-FEB-11
42069|Billabong Complex|62637|5|Briefly described|Map Legend|Archean|Archean|Upper amphibolite facies biotite gneiss, coarse-grained augen gneiss, strongly foliated.||||||07-NOV-08
42069|Billabong Complex|63261|5|Briefly described|p4 Fig. 1, p9 Fig. 5|Archean|Archean|Structural term in this context? Written also as the informal Billabong complex (p7). Age: 2514+/-3Ma.||||||07-FEB-11
42069|Billabong Complex|63866|6|Mentioned|p92|||Southeast Tanami Region.||||||
42069|Billabong Complex|64573|5|Briefly described|p780, p780 Fig. 1|||Geological Province: Tanami Inlier. Leucocratic graintic gneiss was inferred to have a ca 2530Ma igneous precursor.||||||07-FEB-11
42069|Billabong Complex|64662|5|Briefly described|p30 Fig. 3, p44|Archean|Archean|Shown informally as Billabong complex (p30 Fig. 3). Age: 2514+/-3Ma. Geological Province: Tanami region. Possible source of Archean detrital zircons in Ferdies Member, Dead Bullock Formation.||||||07-FEB-11
42069|Billabong Complex|64722|5|Briefly described|Fig. 2 p3-6, p10|Neoarchean|Neoarchean|Of the Tanami Region.|~2510 Ma.|||||11-APR-12
42069|Billabong Complex|64734|5|Briefly described|p187, p186 Fig.1|Neoarchean||~2510 Ma; basement rocks in the Tanami Region; banded granitic gneisses||||||14-SEP-09
42069|Billabong Complex|65232|6|Mentioned|p2|||Archaean basement inlier. Tanami Region||||||09-FEB-10
42069|Billabong Complex|65358|5|Briefly described|p6|Neoarchean|Neoarchean|Basement in Tanami Region. Includes 2520-2500 Ma amphibolite facies gneiss and metasediments.||||||
42069|Billabong Complex|66129|6|Mentioned|p216 Fig.3|Neoarchean|Neoarchean|Unconformably underlies Dead Bullock Formation. 2514 +/- 3 Ma.||||||
42069|Billabong Complex|66468|5|Briefly described|p16-17, p27|Neoarchean|Neoarchean|2514 +/- 3 Ma (Crispe et al., 2007). Unconformably underlies Dead Bullock Formation.||||||
42069|Billabong Complex|66683|5|Briefly described|p365, p377.|Neoarchean|Neoarchean|Tanami Region. Part of felsic basement to North Australian Craton.|2514 +/- 3 Ma. |||Is overlain by Ferdies Member.||
42069|Billabong Complex|67165|5|Briefly described|Map legend.|Archean|Archean||||||Upper amphibolite facies biotite gneiss, coarse-grained augen gneiss, strongly foliated.|
42069|Billabong Complex|67479|6|Mentioned|p56|||||||||
42069|Billabong Complex|67779|5|Briefly described|p117.|Neoarchean|Neoarchean|Tanami Region. Correlated with Kukalak Gneiss.|2514 +/- 3 Ma (Page et al. 1995).|||||
42069|Billabong Complex|67824|5|Briefly described|p384-386 Figs.1-3, p387|Neoarchean|Neoarchean|Oldest exposed rocks in the Tanami region.|2514 +/- 3 Ma (Page et al., 1995).|||Overlain by the Tanami Group.|High grade metasedimentary rocks and leucogranites.|
42069|Billabong Complex|67826|6|Mentioned|p400, p402 Fig.3|Neoarchean|Neoarchean|Oldest known rocks of the Tanami region. Basement. Age determined using 207Pb/206Pb zircon dating.|2514 +/- 3 Ma||||Gneisses.|
42069|Billabong Complex|68474|6|Mentioned|p572, p574|Neoarchaean|Neoarchaean|Granites-Tanami Orogen. Oldest rocks in the Orogen.|ca. 2514 +/- 3 Ma ||||Leucocratic orthogneiss and schistose metasedimentary and felsic volcanic rocks.|
42069|Billabong Complex|68733|5|Briefly described|p186, p187 Fig.6|Neoarchean|Neoarchean|||||Unconformably overlain by the Tanami Group.||
42069|Billabong Complex|68998|5|Briefly described|vi, p1, p31-34, Appendix Tb.11|||SW of De Bavay Hills. The only known Archaean rocks exposed in the Tanami Region. Crops out as a few small tors and pavements. Another age of 2510 +/- 4 Ma was derived from zircon rims and solitary grains. Metamorphism and/or recrystallisation of the igneous protolith occurred at 2481 +/- 7 Ma and c.1805 Ma. Previous age determinations discussed.|2532 +/- 3 Ma (zircon cores).||||Granite gneiss: banded quartz-feldspar-biotite-tourmaline granite, phenocrystic feldspar-quartz-biotite gneissic granite, thin quartz-feldspar-rich leucocratic bands and associatd mica-rich melanosomes.|
42069|Billabong Complex|69003|5|Briefly described|p2, p17|Neoarchean|Neoarchean|Granites-Tanami Orogen.|c.2514 Ma.|||Is overlain unconformably by Dead Bullock Formation.|High-grade metasedimentary rocks and leucogranites.|
42069|Billabong Complex|69031|6|Mentioned|p3|||North Australian Craton.||||||
42069|Billabong Complex|69253|6|Mentioned|p748 Fig.2|Neoarchean|Neoarchean||2514 +/- 3 Ma.|||||
42069|Billabong Complex|69419|5|Briefly described|p4:7,|Neoarchean|Neoarchean|Page et al. (1995). Tanami Region. Limited exposure, immediately S of De Bavay Hills, but extends undercover c.200 km2. SHRIMP U-Pb zircon age; there are also inherited zircons aged c.2550 and 2530 Ma.|2514 +/- 3 Ma (Page et al., 1995).||||Banded quartz-feldspar-biotite-tourmaline gneissic granite (amphibolite facies); thin quartz-feldspar-rich leucocratic bands and associated mica-rich melanosomes.|12-JUL-16
42069|Billabong Complex|69426|5|Briefly described|p11:3-5, 13|Archean|Archean|See also the reference to the informally-named Billabong complex also on p3. Underwent upper-amphibolite facies metamorphism prior to deposition of the Tanami Group.|||||Granite and gneiss.|12-JUL-16
42069|Billabong Complex|69537|5|Briefly described|iv, p1-7|Archean|Archean|Tanami Region. Outcrop is limited to a few small tors and pavements; mostly covered by unconsolidated sand. Granitic gneiss was sampled for zircons to be dated. Previous age (Page et al., 1995) of 2514 +/- 3 Ma. This study found ages of 2532 +/- 3 Ma and 2510 +/- 4 Ma; possibilites include a combination of inheritance and crystallisation, or crystallisation and metamorphism. Similarity with Pine Creek Orogen ages suggests an extensive Neoarchean basement underlying much of the North Australian Craton.|||||Granite, gneissic granite, quartz-feldspar-rich leucocratic bands and associated mica-rich melanosomes.|
42069|Billabong Complex|69618|6|Mentioned|p91 Fig.2, p100 Fig.10||||2514 +/- 3 Ma.|||||
42069|Billabong Complex|69747|5|Briefly described|p264-265|Neoarchean|Neoarchean|Geological province: Granites-Tanami Orogen. Oldest known rocks in the GTO.|2514+\-3 Ma||||Leucocratic orthogneiss and metasedimentary rocks.|
42069|Billabong Complex|70291|4|Described|p179|Neoarchean|Neoarchean|Geological province: Tanami. Oldest rocks in the Tanami region.|~2514+\-3 Ma||||Meta-arkose; high-grade metasedimentary rocks (amphibolite-grade and higher) rocks and leucogranites|
42069|Billabong Complex|71256|6|Mentioned|p21|||Tanami region. Includes a significant proportion of low delta18 O magmatic and inherited zircon.||||||
42069|Billabong Complex|71348|6|Mentioned|p217|Neoarchean|Neoarchean|Geological province: Tanami Region, North Australian Craton. Neoarchean basement complex coeval with Neoarchean magmatism at the Gawler Craton.|c. 2530-2510 Ma|||||
42069|Billabong Complex|71349|5|Briefly described|p736|Archean|Archean|Tanami Region.|2514 +/- 3 Ma (Page et al., 1995).||||Granitic plutons.|
42069|Billabong Complex|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|2514+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
42069|Billabong Complex|73089|4|Described|p3, p5, p7, p10, p22, p30-31|Neoarchean|Neoarchean|Granites-Tanami Orogen, southeastern. Poorly exposed; forms rare inlier of Neoarchean basement rock. Geochron interpreted to record magmatic crystallization. Hf and O isotopes of zircon indicate isotopically heterogeneous basement.|2513 +/- 3 Ma, 2510 +/- 4 Ma|||Overlain by Tanami Group.|Includes quartzofeldspathic gneiss, granitic orthogneiss.|
42069|Billabong Complex|73158|5|Briefly described|p2, p9|Archean|Archean|Southeast of the Granites-Tanami Orogen.|2514+/-3 Ma U-Pb zircon||||Granitic gneisses.|
42069|Billabong Complex|73159|5|Briefly described|p2, 9|Archaean|Archaean|Southeast of the Granites-Tanami Orogen.|2514 +/- 3 Ma (U-Pb; Page et al., 1995).||||Granitic gneisses.|
42069|Billabong Complex|73184|6|Mentioned|p192|||Tanami region, Includes Neoarchean crystallisation ages (Joly et al., 2013).||||||
42069|Billabong Complex|73345|6|Mentioned|p228|||||||||
25785|Billeranga Subgroup|24160|4|Described|p21, 25, 26, 28|Proterozoic|Proterozoic|Formerly Billeranga Beds and Billeranga Group. 100 - 400 m thick.|1390 +/- 140 Ma (Rb-Sr isochron:Giddings 1976).|Moora Group|Capalcarra and Neereno Sandstones; Dalaroo Siltstone; Morawa Lavas; Oxley Chert.|Is overlain unconformably by Coomberdale Subgroup.|Sandstone, siltstone, basalt, tuff, contains stromatolites.|
25785|Billeranga Subgroup|24410|5|Briefly described|p142 Tb. 60|||Parts previously mapped as Billeranga Beds and Billeranga Group. Now comprises Capalcarra Sandstone and Dalaroo Siltstone and Neereno Sandstone, Dalaroo Siltstone, Morowa Lavas and Oxley Chert.||||||24-NOV-09
25785|Billeranga Subgroup|40307|6|Mentioned|p62|||||||||
25785|Billeranga Subgroup|40346|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25785|Billeranga Subgroup|40347|2|Defined|p18|Mesoproterozoic|Mesoproterozoic|||||||
25785|Billeranga Subgroup|40349|4|Described|p13|||||||||
25785|Billeranga Subgroup|44138|4|Described|p272|||Weakly deformed immature fluviatile-alluvial fan-basin margin sequence. 100-400m thick over rugged surface. Rb-Sr dates poorly defined.|1000 Ma and 1390 +/- 140 Ma.|Moora Group (lower)||Overlain by Coomberdale Subgroup (disconformably).|Sandstone, siltstone, basalt, tuff.|
25785|Billeranga Subgroup|64580|4|Described|map legend||Mesoproterozoic|Of Moora Group. Sandstone, siltstone, basalt and volcanic sandstone.||||||09-DEC-08
25785|Billeranga Subgroup|70796|5|Briefly described|500k_interpgeop14_lut.csv|Neoproterozoic|Neoproterozoic|Moora Basin, Pinjarra Orogen. Affected by the Leeuwin Orogeny.|ca. 1000  531 Ma (inferred)|Moora Group|||Sandstone, siltstone, basalt and volcaniclastic sandstone.|
25785|Billeranga Subgroup|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, claystone, basalt, sandstone|
25785|Billeranga Subgroup|71269|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Pinjarra Orogen. Of Moora Basin. Events: Leeuwin Orogeny (780-515 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv.|1600-1000 Ma|Unit of Moora Group.|||Sandstone, siltstone, basalt and volcaniclastic sandstone|
25785|Billeranga Subgroup|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Moora Basin.||Moora Group.|||Sandstone, siltstone, basalt and volcaniclastic sandstone.|
79288|Bindoo Sandstone|70826|6|Mentioned|p7 tbl 3|Silurian|Ordovician|Perth Basin.||||||
79288|Bindoo Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Devonian|Silurian|Perth Basin.|||||Description says: Ultramafic volcanic rock; metamorphosed. but Lithology says: Sandstone.|24-APR-20
23389|Binningup Calcrete|40367|4|Described|p81|Holocene|Holocene|Widespread sheet of calcrete. Thickness: 0.3-0.5m. See also Binningup calcrete.||||||07-AUG-07
29906|Birksgate Complex|23483|5|Briefly described|p4|||||||||
29906|Birksgate Complex|24197|5|Briefly described|p97, p98|||Refers to all metamorphic rocks (granulites and amphibolite-facies gneisses) south of Woodroffe Thrust (Fregon Domain) - excl.Giles Complex and Kulgera Supersuite. Includes Wataru Gneiss. Comprises >90% acid lithologies. Geol. Province: Musgrave Block.||||||07-FEB-11
29906|Birksgate Complex|24496|4|Described|p14|Mesoproterozoic|Mesoproterozoic|Includes massive orthogneiss and well layered gneisses, and migmatites. Volcanosedimentary protoliths with ages: ~1550 and ~1300 Ma. Unconformably overlain by Bentley Supergroup. Geological Province: Musgrave Block.||||||03-AUG-09
29906|Birksgate Complex|24497|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Musgrave Block.||||||
29906|Birksgate Complex|24499|5|Briefly described|Map legend|||Of the Bentley Supergroup?||||||
29906|Birksgate Complex|43052|5|Briefly described|p158|||||||||
29906|Birksgate Complex|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Metasediments, gneiss, granulite. Includes Wataru Gneiss. Geological Province: Musgrave Block.||||||07-NOV-08
29906|Birksgate Complex|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
29906|Birksgate Complex|43298|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
29906|Birksgate Complex|43561|6|Mentioned|p1439|||||||||
29906|Birksgate Complex|50607|6|Mentioned|p1.1|||Geological Province: Musgrave Block. Intruded by: Kulgera Supersuite, Winburn Suite.||||||
29906|Birksgate Complex|60660|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes granulite, gneiss, migmatite and granite. Geological Province: Musgrave Block.||||||22-FEB-05
29906|Birksgate Complex|60662|5|Briefly described|Map Legend|||Includes layered granulites.||||||22-FEB-05
29906|Birksgate Complex|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: ~1560-1300Ma. Granulite to amphibolite facies quartzofeldspathic gneiss, felsic to ultramafic orthogneiss, peltic-calcic paragneiss and iron formation.||||||
29906|Birksgate Complex|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Granulite to amphibolite facies quartzofeldspathic gneiss, felsic to ultramafic orthogneiss, pelitic-calcic paragneiss and iron formation. Age: ~1560-1300 Ma.||||||
29906|Birksgate Complex|61524|5|Briefly described|p16|Mesoproterozoic|Mesoproterozoic|Leucocratic quartz-feldspar gneiss, felsic granulite gneiss and melanocratic quartz-hypersthene gneiss. Age: ~1600-1300 Ma. Geological Province: Musgrave Province. See also p17 Fig.1, p18 Fig. 2(a)||||||
29906|Birksgate Complex|61864|5|Briefly described|p18, p19 fig 5|||Part of the basement of Musgrave Province. Sediments and volcanics.|||||Granulite to amphibolite-facies gneiss: para- and orthogneisses with interlayered mafic gneiss.|
29906|Birksgate Complex|64645|5|Briefly described|p16 Fig. 2|Mesoproterozoic|Paleoproterozoic|Age: 1600-1300Ma. Geological Province: Musgrave Province.||||||
29906|Birksgate Complex|64722|5|Briefly described|Fig. 2 p3-6, p16|Calymmian|Calymmian|Oldest exposed unit in Musgrave Orogen. Contains 1600-1500 Ma zircons. Geochemistry suggests subduction related environment to 1555 Ma.|||||Comprises felsic rocks, subordinate mafic units, rare metapelite, quartzite, calcsilicate rock.|11-APR-12
29906|Birksgate Complex|64745|5|Briefly described|p372, p373 Fig. 3, p374 Tab. 1|||Included within informal Musgravian Gneiss in this paper. Geol. Prov: Fregon Domain, Musgrave Province.||||||
29906|Birksgate Complex|64831|5|Briefly described|p1128 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: ca 1590-1550Ma. Comprises felsic, intermediate and mafic gneisses - dominantly felsic orthogneiss with subordinate mafic gneiss, intermediate gneiss and metasedimentary rocks. See also p1131.||||||
29906|Birksgate Complex|65135|6|Mentioned|p5|||Used to describe all rocks deformed during the Musgravian Orogeny by Major and Conor (1993)||||||
29906|Birksgate Complex|65376|6|Mentioned|p9 Fig.1.2. |Mesoproterozoic|Mesoproterozoic||||||Metasedimentary and meta-igneous gneiss.|
29906|Birksgate Complex|65385|5|Briefly described|pS132|Calymmian|Calymmian|~1600-1400 Ma. Intruded by Pitjantjatjara Supersuite.||||||08-MAR-12
29906|Birksgate Complex|65833|6|Mentioned|p5.|||Musgrave area. Of Major and Conor (1993), who included all rocks formed prior to, and metamorphosed during, the 1225-1150 Ma Musgravian Orogeny.||||||
29906|Birksgate Complex|65906|5|Briefly described|p5|Mesoproterozoic|Mesoproterozoic|Large proportion of outcrop in Musgrave Block. Gneisses deposited between 1600-1540 Ma as sedimentary rocks, with volcanics and volcaniclastics. Felsic; island-arc subduction affinities.||||||
29906|Birksgate Complex|67128|6|Mentioned|p6-7|||Includes all gneisses in the eastern Musgrave Province. Some of these were thought to have granitic protoliths up to 1590 +/- 25 Ma old; these now appear to be due to detrital zircon components.||||||
29906|Birksgate Complex|67323|6|Mentioned|Eastern Australia Time-Space Plot|||Musgrave Block.||||||
29906|Birksgate Complex|67375|5|Briefly described|p6, p17. |||Musgrave Province. Included all rocks metamorphosed during the Musgrave Orogeny, including the Mesoproterozoic granite suites and the basement they intruded.||||||
29906|Birksgate Complex|67536|5|Briefly described|Map Legend|||Musgrave Block. Informally subdivided into four parts, one of which is demagnetised or altered gneiss or granulite adjacent to major structures or Giles Complex intrusives. Non-magnetic, weakly magnetic, moderately magnetic, and variably magnetic in parts.|||Includes Wataru Gneiss.||Sheared, altered or granite-intruded gneiss or granulite adjacent to major shear zones; massive mainly meta-igneous gneiss and granulite, may include charnockite/migmatite alteration of layered granulite; layered metasedimentary gneiss and granulite.|02-APR-14
29906|Birksgate Complex|67921|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Shown only in section.|||||Metasediments, gneiss, granulite.|
29906|Birksgate Complex|68100|6|Mentioned|p4, 6 |||Of Major and Conor (1993). Fregon Domain. Includes gneissic basement rocks. Gneissic rocks called Wirku Metamorphics in west Musgrave Province.||||||19-JAN-17
29906|Birksgate Complex|68131|5|Briefly described|p2 Fig.1|Mesoproterozoic|Mesoproterozoic||||||Metasedimentary and meta-igneous gneiss.|
29906|Birksgate Complex|69091|6|Mentioned|p60, p103 Fig.5.6|||In South Australian section of Musgrave Province, all rocks metamorphosed during Musgrave Orogeny, including Mesoproterozoic granite suites and basement through which they intruded, were initially grouped into Birksgate Complex (Major and Conor, 1993). However, recent work has shown that much of what was previously regarded as exposed basement in west Musgrave Province actually comprises supracrustal packages (now mainly paragneiss) deposited between c. 1340 Ma and 1270 Ma (Evins et al., 2012) - referred to as Wirku Metamorphics (Howard et al., 2007; Evins et al., 2009; Smithies et al., 2009).||||||
29906|Birksgate Complex|69213|5|Briefly described|p35, p36 Fig. 12, p28-29 fig.6|||Musgrave Province.|||||Gneisses. Stromatic metatexite migmatite defined by layer parallel, mostly in source leucosomes. Leucosomes of two types; medium grained, straight margined and coarse grained less sharp margined leucosomes.|
29906|Birksgate Complex|69436|6|Mentioned|p21:2-3||||1600-1540 Ma.|||||12-JUL-16
29906|Birksgate Complex|69640|4|Described|p11-p14, p16-p17, p24, p31-p32|Proterozoic|Proterozoic|Musgrave Province. Subsequently deformed and metamorphosed to amphibolite to granulite facies during the ca 1220-1120 Musgrave Orogeny. Petrology, petrographic description, SHRIMP methodology, results and analayses for numerous samples are provided. An additional magmatic crystallisation age of 1617 +/- 8 Ma was obtained. A maximum depositional age of 1588 +/- 7 Ma was also obtained for a quartzo-feldspathic gneiss. Metamorphic ages inculding 1158 +/- 8 Ma are provided. See also p50, p57, p65, p73-p74, p79, p137, p141, p145, p157.|1605 +/- 6 Ma (SHRIMP, magmatic crystallisation)|||Intruded by the Pitjantjatjara Supersuite.|Felsic ortho- and paragneisses including biotite quartzo-feldspathic paragneiss, hornblende-biotite-diopside quartzo-feldspathic gneiss, migmatitic gneiss.|
29906|Birksgate Complex|69729|5|Briefly described|p67, p88|||Major and Conor (1993), for west Musgrave Province basement defined as rock metamorphosed during the Musgrave Orogeny. These were reassigned (Howard et al., 2009) to Wirku Metamorphics on the basis of geochronology (discussed).||||||
29906|Birksgate Complex|70083|5|Briefly described|p206-208, 229|||The name used for the Musgravian Gneiss in the Fregon Subdomain, Eastern Musgrave Inlier, Musgrave-Albany-Fraser Orogen. Is termed the Olia Gneiss in the Mulga Park Subdomain.|||Kalamurta Gneissic Unit.|Is dissected (intruded) by Alcurra Dolerite dykes.|Peraluminous metapelite gneiss, intercalated with more quartzofeldspathic, and granitic gneisses.|12-MAY-23
29906|Birksgate Complex|70338|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Part of the basement to the Musgrave Province. The five facies are mapped separately.|||||Gneiss, granulite and amphibolite facies S of the Woodroffe Thrust. Pale brown, quartzo-feldspathic granofels; layered, quartzo-feldspathic orthogneiss to leucogneiss; layered to migmatitic, quartzo-feldspathic paragneiss; meta-calcsilicate rock.|
29906|Birksgate Complex|70634|6|Mentioned|189540.1.pdf|||Now named Wirku Metamorphics.||||||
29906|Birksgate Complex|71170|5|Briefly described|p9, p23|||Musgrave Province. Name derived from Major and Conor, 1993.||||||
29906|Birksgate Complex|71321|4|Described|p1-2,4-5,8,14,17-18,21,24|Calymmian|Statherian|Geological province: Musgrave Province. Comprises part of basement, and oldest rocks exposed on the Musgrave Province. Occurs in outcrop as blocks or rafts (several cm to hundreds of meters across) within Pintjantjatjara Supersuite. See p14-17 for detailed descriptions of outcrop. Deformed (early gneissic layering and folding) and metamorphosed to amphibolite to granulite facies during c. 1220-1120 Ma Musgravian Orogeny. Intruded by granitoid bodies of Pintjantjatjara Supersuite. Geochemically similar to c. 1345-1293 Ma Wankanki Supersuite granites in the West Musgrave Province (strong compositional similarities to Phanerozoic granites of the Andean continental arc (Smithies, et al., 2010). Dominantly metaluminous, to slightly peraluminous and predominantly magnesian character; strong affinity to I-type granites. Likely formed in a volcanic arc setting. Has c. 1620-1550 Ma zircons indicating igneous protolith age (Camacho and Fanning, 1995; Edgoose, et al., 1993; Edgoose, et al., 2004; Scrimgeour, et al., 1999); protolith magmatic ages as early as c. 1665 Ma from adjacent AGNES CREEK mapsheet. Emplacement ages in the HANGING KNOLL map include c. 1480 Ma and c. 1440 Ma. Nd and Hf isotopic analysis indicate a relatively juvenile source for both para- and orthogneisses. Considered prospective for Zn-Pb-Ag ore bodies similar to Broken Hill. See also p32-41,55-56,60-63,66-67,74.|c. 1630-1560 Ma||||Felsic and mafic orthogneisses and felsic volcanics, volcaniclastics and paragneisses.|
29906|Birksgate Complex|71322|5|Briefly described|p11-19, p26, p28|||Musgrave Province. Hosts Cu mineralisation at the Kenmore II prospect. Summary log for drillhole DD10WOD007. Leococratic migmatite dated. Metamorphosed at 1180 +/- 5 Ma and 1159 +/- 7 Ma.|1520 +/- 9 Ma (maximum depositional age).||||Intermediate to felsic migmatitic gneisses, paragneisses, orthogneisses and intrusive magmatic rocks, calcsilicate, schist.|13-DEC-21
29906|Birksgate Complex|71416|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|The six facies are mapped separately. Most have protolith ages given. Metamorphosed between c.1170 Ma and 1138 Ma. Solid geology interpretation: demagnetised or altered adjacent to major structures or Giles Complex intrusives; non-magnetic, weakly or variably magnetic.|c.1716 Ma - 1565 Ma.|||Correlative of Kalamurta gneiss.|Quartzo-feldspathic paragneiss, commonly migmatitic; mixed felsic +/- mafic gneiss; amphibolite to granulite facies felsic gneiss, commonly migmatitic; leucocratic diatexite; mafic gneiss, locally migmatitic; undivided gneiss, locally migmatitic.|
29906|Birksgate Complex|71536|6|Mentioned|p73, p78|||Was likely the protolith of the 1143 +/- 9 Ma felsic gneiss in the Pitjantjatjara Supersuite.||||||
29906|Birksgate Complex|71592|5|Briefly described|Appendix A.|||Musgrave Province. Over 20 age determinations are given for crystallisation (within this range), provenance clusters and metamorphism.|1617+/-8 Ma to 1564+/-5 Ma.||||Gneiss, syenogranitic gneiss, granite, monzogranite, pelitic to semipelitic migmatite.|
29906|Birksgate Complex|72238|5|Briefly described|p38|Calymmian|Statherian|Geological province: Musgrave Province. Intruded by Amata Dolerite.|c. 1.7-1.5 Ga|||||
29906|Birksgate Complex|72242|6|Mentioned|p27|Calymmian|Statherian|Geological province: Musgrave Province. Associated with Kararan Orogeny. Coeval with Hiltaba Suite and Toolgana Supersuite, and extensive oceanic crust formation.||||||
29906|Birksgate Complex|72344|6|Mentioned|p28|Calymmian|Statherian|Musgrave Province.|c. 1565-1665 Ma (Jagodzinski et al, 2013)|||Time equivalent to the Toolgana Supersuite.||
29906|Birksgate Complex|72476|5|Briefly described|p24, 27|||Dominant basement unit in eastern Musgrave Province.|~1650-1550 Ma.||||Granulite to upper amphibolite facies, volcanic-dominated supracrustal rocks and felsic intrusives (granites through to tonalites, minor intercalated mafics), with minor sedimentary rocks.|
29906|Birksgate Complex|73100|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Subsurface.|||||Metasediments, gneiss, granulite.|
29906|Birksgate Complex|73109|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Drexel et al. (1993). Subsurface.|||||Metasediments, gneiss, granulite.|
29906|Birksgate Complex|73111|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Subsurface.|||||Metasediments, gneiss, granulite.|
29906|Birksgate Complex|73232|6|Mentioned|p5|||Musgrave Province. This unit dominates the province.||||Intruded by Pitjantjatjara Supersuite and Giles Complex including Alcurra Dolerite.|Deformed and metamorphosed gneissic rocks.|
29906|Birksgate Complex|73234|6|Mentioned|p19|Calymmian|Statherian|Musgrave Province, eastern.|c. 1700-1550 Ma||||Meta-igneous and metasedimentary rocks.|
39507|Bishop Creek Monzogranite|63417|5|Briefly described|Map legend|Archean|Archean|Of the Cleland Supersuite. Geological Province: Pilbara Craton. Biotite monzogranite to granodiorite and syenogranite; fine- to coarse-grained; locally seriate and porhyritic; rare pegmatite dykes; weakly metamorphosed.||||||07-NOV-08
39507|Bishop Creek Monzogranite|63441|5|Briefly described|p9 Tb. 2|Archean|Archean|Of the Cleland Supersuite. Ages: from 3246 +/- 3 to c. 3240 Ma. Geological Province: Pilbara Craton.||||||15-APR-13
39507|Bishop Creek Monzogranite|64621|5|Briefly described|Map legend|Archean|Archean|Of the Cleland Supersuite. Age: 3246-3220Ma. Biotite monzogranite to granodiorite and syenogranite; fine- to coarse-grained, locally seriate and porphyritic; rare pegmatite dykes; metamorphosed.||||||07-NOV-08
39507|Bishop Creek Monzogranite|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.|c.3246 - 3241 Ma (Nelson 2000).|Of Mount Edgar Granitoid Complex.|||Biotite monzogranite to granodiorite, and syenogranite; fine- to coarse-grained, locally seriate and porphyritic; rare pegmatite dykes.|
39507|Bishop Creek Monzogranite|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. This unit was shown as part of the Mount Edgar Granitoid Complex in Version 1 of this map sheet (see Refid 65726).|c.3240 Ma.|Of Cleland Supersuite.|||Biotite monzogranite to granodiorite, and syenogranite; fine- to coarse-grained, locally seriate and porphyritic; rare pegmatite dykes; weakly metamorphosed.|
39507|Bishop Creek Monzogranite|65827|2|Defined|p6 Tb.2, p13 Tb.4, p16, p26, p29, p57|Paleoarchean|Paleoarchean|New name. 40 x 26 km WNW-trending intrusion in the Mount Edgar Granitic Complex. 3246 +/ -3 (SHRIMP U-Pb zircon; Nelson 2005) to 3241 +/- 3 Ma (SHRIMP U-Pb zircon; Nelson 2000). Of Cleland Supersuite. Intruded by Moolyella Monzogranite; intrudes Munganbrina Monzogranite, Coppin Gap, Mullugunya, Zulu, Kennell and Joorina Granodiorites. Non- to weakly-foliated, porphyritic and seriate, fine- to coarse-grained, grey to pink-grey biotite(-muscovite) monzogranite, granodiorite and syenogranite.||||||
39507|Bishop Creek Monzogranite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Cleland Supersuite. 3246-3223 Ma. Biotite monzogranite to granodiorite and syenogranite; fine- to coarse-grained; locally seriate and porphyritic; rare pegmatite dykes; weakly metamorphosed.||||||
39507|Bishop Creek Monzogranite|66217|5|Briefly described|p33.|Paleoarchean|Paleoarchean||c.3240 Ma.|Unit in Cleland Supersuite.||Intrudes Munganbrina Monzogranite.||
39507|Bishop Creek Monzogranite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Age derived from samples of monzogranite and granodiorite (178076.1.pdf, 169036.1.pdf). Intruded by unnamed k feldspar porphryitic dyke.|3223 +/- 3 Ma - 3294 +/- 5 Ma (SHRIMP)|Cleland Supersuite|||Biotite monzogranite to granodiorite and syenogranite; fine to coarse grained; locally seriate and porphyritic; rare pegmatite dykes; weakly metamorphosed|
39507|Bishop Creek Monzogranite|69566|6|Mentioned|p236|||Mount Edgar Granitoid Complex, East Pilbara Granite-Greenstone Terrane.||Cleland Supersuite.||||
39507|Bishop Creek Monzogranite|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA 142983 (biotite monzogranite) yielded an interpreted igneous crystallisation age of 3241+\-3 Ma (weighted mean 207Pb/206Pb). Sample GSWA 169034 (biotite monzogranite) yielded an interpreted igneous crystallisation age of 3236+\-3 Ma for the monzogranite (weighted mean 207Pb/206Pb). Sample GSWA 169036 (biotite granodiorite) yielded an interpreted igneous crystallisation age of 3294+\-5 Ma for the granodiorite (weighted mean 207Pb/206Pb). Sample GSWA 178076 (biotite monzogranite) yielded an interpreted igneous crystallisation age of 3223+\-3 Ma for themonzogranite (weighted mean 207Pb/206Pb). Sample GSWA 178094(biotite monzogranite) yielded an interpreted igneous crystallisation age of 3243+\-5 Ma for themonzogranite (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3252-3224 Ma (inferred)|Unit of Cleland Supersuite.|||Biotite monzogranite to granodiorite and syenogranite; fine to coarse grained; locally seriate and porphyritic; rare pegmatite dykes; weakly metamorphosed|
39507|Bishop Creek Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, granodiorite, syenogranite|
39507|Bishop Creek Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||Max age 3246+/-3 Ma, min 3223+/-3 Ma.|Cleland Supersuite|||Biotite monzogranite to granodiorite and syenogranite; fine to coarse grained; locally seriate and porphyritic; rare pegmatite dykes; weakly metamorphosed.|
83457|Bit Basher Shale|73513|4|Described|p31, p35, p36 Fig.9, p40|||Perth Basin. Informal name for genetically distinct upper interval in High Cliff Sandstone, correlated throughout northern part of the basin. Lower shoreface to inner shelf environment.||High Cliff Sandstone||Underlies Kingia Sandstone|Highly bioturbated and storm re-worked argillaceous sandstone and siltstone. Distinct base and top, variable thickness of 5-50 m.|
79261|Bitter Springs Group|70762|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Amadeus Basin, Centralian Superbasin.||||Overlies Heavitree Quartzite.|Dolomite, stromatolitic dolomite, siltstone, and sandstone; evaporitic in subsurface.|
79261|Bitter Springs Group|71001|5|Briefly described|p16-18, 20, 22, 25-26, 28|Tonian|Tonian|Amadeus Basin. Formerly Bitter Springs Formation, the Members of which are now Formations of the Bitter Springs Group. Shallow-marine, lagoonal and supratidal environments. Age determinations vary.|~830-750 Ma.||Gillen, Johnnys Creek, Loves Creek Formations.|Overlies Heavitree Quartzite. Is overlain by Areyonga Formation.|Thick halite and sulfate evaporite accumulations.|
79261|Bitter Springs Group|71080|5|Briefly described|p4, p9, 23, 26, 27, p29 Fig 20, p30, 31|Tonian|Tonian|Amadeus Basin. Supersequence 1.|||Includes Gillen Formation, Loves Creek Formation, Johnnys Creek Formation.|Overlies Heavitree Formation.||
79261|Bitter Springs Group|71268|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Of Amadeus Basin (Phase 1), Centralian Superbasin. [Also referred to as Bitter Springs Formation]. Events: Delamerian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma). See 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv.|900-720 Ma (inferred)||Includes Johnnys Creek Formation.|Underlain by Dean Quartzite. Equivalent to Pinyanna beds.|Phyllitic schist, locally sericitic phyllonite; derived from siltstone and mudstone; dolomite, stromatolitic dolomite, siltstone, and sandstone; evaporitic in subsurface.|
79261|Bitter Springs Group|71279|5|Briefly described|p355 Fig.2, p364, p366-367|||A structurally-complex, salt-rich sedimentary package.|||Gillen, Loves Creek, Johnnys Creek, Formations.||Salty shale, chert, dolostone and limestone.|
79261|Bitter Springs Group|71344|5|Briefly described|p1092, 1093 Fig 1|Neoproterozoic|Neoproterozoic|Amadeus Basin.|575- 565 Ma|||||
79261|Bitter Springs Group|71810|5|Briefly described|Map legend.|Tonian|Tonian|Amadeus Basin (Phase 1), Centralian Superbasin.|<896 Ma.|||Overlies Heavitree Formation. Is overlain by Carnegie Formation.|Dolomite, stromatolitic dolomite, siltstone, and sandstone; evaporites in subsurface.|
79261|Bitter Springs Group|71841|5|Briefly described|iii,p1-2|Cryogenian|Cryogenian|Of Amadeus Basin. Previously termed Bitter Springs Formation. Status upgraded to Group and formalised by Normington et al (2015), Normington and Donnellan (in review). |||Includes Johnnys Creek, Loves Creek and Gillen formations.|Overlain by Inindia beds or Areyonga Formation. Grades into Pinyanna beds.||
79261|Bitter Springs Group|71842|5|Briefly described|iii,p2-5,9|Cryogenian|Cryogenian|Of Amadeus Basin. Part of revised nomenclature after this study in the Mount Conner area.|||Includes Johnnys Creek Formation, Loves Creek Formation and Gillen Formation.|Underlain by Dean Quartzite or Heavitree Quartzite.||
79261|Bitter Springs Group|71898|5|Briefly described|p9|||Amadeus Basin.|||Includes the Loves Creek Formation.|Unconformably overlain by the Tempe Formation.||
79261|Bitter Springs Group|72034|5|Briefly described|500k_interpgeop16_lut|Tonian|Neoproterozoic|Amadeus Basin (Phase 1).  Age from biostratigraphy.|||||Dolomite, stromatolitic dolomite, siltstone, sandstone; evaporitic in subsurface.|
79261|Bitter Springs Group|72094|6|Mentioned|p3 Fig 2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||14-APR-22
79261|Bitter Springs Group|72259|6|Mentioned|p10|||Spilitic volcanic rocks occur at the top of the unit. These post-date the negative d13C anomaly dated at ca. 810-790 Ma.|||||Includes spilitic volcanic rocks.|
79261|Bitter Springs Group|72369|5|Briefly described|p15,43|||Of Amadeus Basin.|||Includes Gillen, Loves Creek and Johnnys Creek formations.|Overlain by Winnall Group.|Dolostone, limestone, siltstone, sandstone, halite, evaporites, and a basaltic unit (green-grey to red, fine-grained, and typically shows chlorite-carbonate alteration).|
79261|Bitter Springs Group|72374|5|Briefly described|p6|||Of Amadeus Basin.||||Overlain by Areyonga Formation.||
79261|Bitter Springs Group|72375|4|Described|p2,7,9-11,13,15,17,23|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Nomenclature of Normington et al., 2015 (after Wells et al., 1967). Structurally interleaved with Aileron Province basement rocks; isoclinally infolded with Atneequa Suite and Moonlight Gneiss on LIMBLA and ILLOGWA CREEK mapsheets. Depositional age constrained at c. 820 Ma, based on geochemical affinities with c. 824 Ma Amata Dolerite (Glikson et al., 1996).|||Includes Gillen Formation, Loves Creek Formation, Johnnys Creek Formation.|Overlain disconformably by Wallara Formation.|Predominantly of dolostone, limestone, siltstone, sandstone, halite, evaporite and a rare basaltic unit near the top of the sequence.|
79261|Bitter Springs Group|72489|4|Described|p3, p4 Fig.3, p5-7, p7 Fig.6|Tonian|Tonian|Amadeus Basin, including the Limbla Syncline. Thickness c. 1000m.  See also p8 Fig.7, p9-12. Contains REE record that is evidence of either a non-marine environment or an extremely different ocean chemistry. Age of 13C excursion constrained to 811-785 Ma (through international correlations).|||Includes Gillen Formation,  Loves Creek Formation, Johnnys Creek Formation.|Underlies Areyonga Formation. Overlies the Heavitree Formation.|Includes carbonate and siliciclastic succession.|14-SEP-20
79261|Bitter Springs Group|72516|5|Briefly described|p85-86|Tonian|Tonian|Amadeus Basin. Formerly the Bitter Springs Formation.  Correlated with the Yackah beds. Both units contain a columnar, branching stromatolite Acaciella australica. Min age ~820 Ma from intruding dykes.|Ca 820 Ma min age?|||Overlies the Heavitree Formation.||14-APR-22
79261|Bitter Springs Group|72601|5|Briefly described|p3, p7, p10-12, p14, p17, p25|Tonian|Tonian|Amadeus Basin. Previously called the Bitter Springs Formation. Contains diverse Tonian biotic assemblages [palynomorphs].|||Johnnys Creek Formation, Loves Creek Foramtion, Gillen Formation|Underlain by Heavitree Formation and Dean Quartzite. Unconformably overlain by Wallara Formation.|Carbonate rocks with fine siliciclastic interbeds.|
79261|Bitter Springs Group|72714|6|Mentioned|p2, p4|||Amadeus Basin. Regionally, copper-bearing fluorite veins are found on the contact between the Atneequa Suite and overlying Heavitree Formation and Bitter Springs Group. Listed as Bitter Springs Formation p2.||||||
79261|Bitter Springs Group|73085|5|Briefly described|piii, p1-2, p4, p15-16, p27|Tonian|Tonian|Amadeus Basin. Previously called Heavitree Quartzite.|||Johnnys Creek Formation, Loves Creek Formation, Gillen Formation|Underlain by Dean Quartzite and Heavitree Formation. Unconformably[?] overlain by Wallara Formation.||
79261|Bitter Springs Group|73086|1|Redefined|[See comments].|Tonian|Tonian|[Redefined herein. See also definition card, ASUD]. Re-definition of unit/upgrade from formation to group. Amadeus Basin. Part of Supersequence I; deposited during the early sag phase of basin development. The base is taken to be the first thick (~1 m) shale interval above the Heavitree Formation. Top of the unit coincides with a sequence boundary with up to 200 m relief and is impacted by salt tectonism which caused thickening [etc]. Metamorphosed up to lower amphibolite facies in the Arltunga and Ormiston nappe complexes. Complex folding and faulting are widespread problems with assigning a recognisably complete type or reference section. ~790 m thick at the Ellery Creek type area but the true thickness is difficult to ascertain due to complex structure resulting from orogenesis and halotectonics. Max thickness: 1651.5 m (Murphy-1 drillhole). Stromatolites are present in all constituent formations. Poorly constrained minimum age of ca 820 Ma. Maximum age is less well constrained; globally synchronous carbon isotopic signatures indicate an age range of 815-787 Ma for the unit. Deposited on a shallow, stable shelf with a minor amount of fine-grained siliciclastic input. Areyonga Movement resulted in uplift and erosion of parts of the Heavitree - Wallara Formation succession. May correlate to Pinyinna beds, Yackah beds, Lewis Range Sandstone, Young Husband Conglomerate, Coominaree Dolomite and Browne Formation. p: iii, 3, 5-11, 14-18, 29-30, 35, 38-40, 49, 53, 57, ~62-68, 70, 72, 100-105, 113,  130, ~143-154, 157, 160, 167, 171, App 2.|Between ca. 1000 Ma and ca. 820 Ma.||Gillen Formation, Loves Creek Formation, Johnneys Creek Formation|Conformable/transitional [in places] contact with the underlying Heavietree Formation. Overlain by Wallara Formation, Areyonga Beds[Formation?], Olympic Formation. [See comments].|Dolostone, limestone and cherty limestone, with subordinate sandstone, red and green siltstone and black shale. Where metamorphosed, the rocks are slate, phyllite, schist, and calc-silicates.|
79261|Bitter Springs Group|73088|6|Mentioned|piii, p1-2, p4, p12|Tonian|Tonian|Amadeus Basin. Present in drillhole BL002. Previously called Bitter Springs Formation.|||Johnnys Creek Formation, Loves Creek Formation, Gillen Formation|Underlain by Heavitree Formation. Overlain by Wallara Formation.|Includes dolostone and dolomitic siltstone.|
79261|Bitter Springs Group|73180|6|Mentioned|p48 Fig.1, p49-51, p53|Neoproterozoic|Neoproterozoic|Amadeus Basin. Disconformable contact with the overlying Areyonga Formation in the east side of the basin where a step-like scour demarcates the western limit of the Sturt ice-sheet, or where it changed from grounded to floating. A narrow, deep valley-like feature observed in seismic images cuts through the upper Bitter Springs Group before terminating in salt within the Gillen Formation, resembles sub-glacial tunnel valleys. Local scouring of the Base Areyonga Disconformity into the Bitter Springs Group suggests locations where the generally floating Sturt ice-sheet grounded. Unconformably underlies the Olympic Formation and Pioneer Formation.|||Gillen Formation, Loves Creek Formation, Johnnys Creek Formation|Conformably overlies the Heavitree Quartzite, Dean Quartzite. Disconformably underlies the Wallara Formation and Areyonga Formation.||
79261|Bitter Springs Group|73338|6|Mentioned|p5, p8|||Unconformably overlies basement in the Mount Kitty 1 well.|||Gillen Formation|||
79261|Bitter Springs Group|73346|6|Mentioned|p5, p28|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
79261|Bitter Springs Group|73437|6|Mentioned|p151|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
79261|Bitter Springs Group|73445|5|Briefly described|p10, 56, 58|Neoproterozoic|Neoproterozoic|Amadeus Basin. Hosts SEDEX-style base metal mineralisation (Enceladus and Iapetus prospects).||||||
79290|Black Dragon Gneiss|69595|5|Briefly described|p5, p6|Statherian|Orosirian||c. 1815-1800 Ma||||Metagranitic gneiss.|
79290|Black Dragon Gneiss|70089|6|Mentioned|p263|Paleoproterozoic|Paleoproterozoic|Biranup Zone, NE Albany-Fraser Orogen.|||||Metagranodiorite and metadiorite.|
79290|Black Dragon Gneiss|70182|5|Briefly described|p4-5, p14|Paleoproterozoic|Paleoproterozoic|Doyle et al. (2014). Tropicana Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen.|c.1815 Ma (protoliths).||||Metagranodiorite and metadiorite.|
79290|Black Dragon Gneiss|70256|5|Briefly described|p4-5|||Blenkinsop and Doyle (2014). Biranup Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen.|1815-1800 Ma.||||Metagranodiorite, quartz metadiorite, metadiorite.|
79290|Black Dragon Gneiss|70802|5|Briefly described|250k_pre_mesozoic_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Biranup Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage II (1225-1140 Ma); Albany-Fraser Orogeny (1330-1140 Ma); Albany-Fraser Orogeny Stage I (1330-1260 Ma); Biranup Orogeny (1710-1620 Ma); Zanthus Event (1680-1675 Ma); Ngadju Event (1780-1760 Ma); Salmon Gums Event (1815-1800 Ma).|1815-1790 Ma (inferred)||||Metagranodiorite and metadiorite; may include remnants of Archean rocks and Tropicana Gneiss|
79290|Black Dragon Gneiss|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Biranup Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen.||||May include remnants of Archean rocks and Tropicana Gneiss.|Metagranodiorite and metadiorite; may include remnants of Archean rocks and Tropicana Gneiss.|
31068|Black Duck Tonalite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of Dougalls suite.  Age c. 1850 Ma||||||07-NOV-08
31068|Black Duck Tonalite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tickalara Metamorphics (Lamboo Complex).  Age: 1865-1850Ma.||||||07-NOV-08
31068|Black Duck Tonalite|43854|5|Briefly described|Map Legend||Proterozoic|||||||
31068|Black Duck Tonalite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31068|Black Duck Tonalite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Dougalls Suite|||Foliated leucocratic biotite-muscovite(-epidote) metatonalite to metagranodiorite; inclusions of epidote amphibolite.|30-JUL-15
31068|Black Duck Tonalite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Dougalls Suite|||Foliated leucocratic biotite--muscovite(--epidote) metatonalite to metagranodiorite; inclusions of epidote amphibolite.|
31068|Black Duck Tonalite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Central Zone.|1849-1849 Ma (Inferred)|Unit of Dougalls Suite.|||Foliated leucocratic biotite-muscovite(-epidote) metatonalite to metagranodiorite; inclusions of epidote amphibolite|
31068|Black Duck Tonalite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1849 Ma (inferred)|Unit of Dougalls Suite.|||Foliated leucocratic biotite-muscovite(-epidote) metatonalite to metagranodiorite; inclusions of epidote amphibolite|
28372|Black Flag Group|7471|6|Mentioned|p23|||Kalgoorlie Terrane. Has steep REE pattern, not ideal for volcanic-hosted massive sulfide mineralisation.|||||Dacites and rhyolites.|
28372|Black Flag Group|22534|4|Described|Fig.4 p7||Archean|See also Table 2 p8.||||||07-NOV-08
28372|Black Flag Group|22596|6|Mentioned|Fig.9 p419|||||||||
28372|Black Flag Group|22666|5|Briefly described|p696, Fig.1b|||||||||
28372|Black Flag Group|22682|5|Briefly described|p13||Archean|Corresponds to Black Flag Supersequence.||||||07-NOV-08
28372|Black Flag Group|23137|4|Described|p245 Table.2|||||||||
28372|Black Flag Group|23141|6|Mentioned|p216|||||||||
28372|Black Flag Group|23142|5|Briefly described|p202|||||||||
28372|Black Flag Group|23795|6|Mentioned|p11|||Geological Province: Yilgarn Craton.||||||
28372|Black Flag Group|23796|6|Mentioned|p31|||||||||
28372|Black Flag Group|23853|5|Briefly described|p834|||||||||
28372|Black Flag Group|23926|6|Mentioned|p16 Fig. 5|||||||||
28372|Black Flag Group|24135|6|Mentioned|p17|||||||||
28372|Black Flag Group|24139|5|Briefly described|p235, 237, 253|Archean|Archean|Geological Province: Yilgarn Craton. Maximum Thickness: ~2500m.  Age: 2666 +/- 6Ma to 2729 +/- 9Ma.||||||07-NOV-08
28372|Black Flag Group|24196|6|Mentioned|p31, p94|||||||||
28372|Black Flag Group|24305|5|Briefly described|p919|||||||||
28372|Black Flag Group|41368|6|Mentioned|Fig.1|||||||||
28372|Black Flag Group|41644|6|Mentioned|p219|||||||||
28372|Black Flag Group|41670|6|Mentioned|p249|||||||||
28372|Black Flag Group|41890|5|Briefly described|p278|||||||||
28372|Black Flag Group|42221|5|Briefly described|p10|||||||||
28372|Black Flag Group|42344|5|Briefly described|p52|||||||||
28372|Black Flag Group|42382|6|Mentioned|Table 1 P9|||||||||
28372|Black Flag Group|42406|5|Briefly described|Fig.2 P250|||||||||
28372|Black Flag Group|42436|5|Briefly described|p73|||||||||
28372|Black Flag Group|42696|6|Mentioned|Plate 1B|Archean||||||||07-NOV-08
28372|Black Flag Group|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
28372|Black Flag Group|42870|5|Briefly described|Table 1, P67|||||||||
28372|Black Flag Group|42892|5|Briefly described|p52|||||||||
28372|Black Flag Group|42989|5|Briefly described|Table 1|||||||||
28372|Black Flag Group|43052|5|Briefly described|Fig.3.8|||||||||
28372|Black Flag Group|43074|6|Mentioned|Table 1|||||||||
28372|Black Flag Group|43101|5|Briefly described|Table 1.|||||||||
28372|Black Flag Group|43102|6|Mentioned|p4|||||||||
28372|Black Flag Group|43125|6|Mentioned|Table 1|||||||||03-MAR-10
28372|Black Flag Group|43162|6|Mentioned|5|||||||||
28372|Black Flag Group|43496|6|Mentioned|12|||U-Pb Age: 2704+/-8Ma||||||
28372|Black Flag Group|50421|4|Described|p285||Archean|Suite of felsic volcanics intercalated with volcaniclastic sedimentary (mud-, silt-, and sandstone) rocks. Kalgoorlie Terrane. Unconformably overlain by Kurrawang Formation and Merougil Formation.||||||09-OCT-12
28372|Black Flag Group|50548|4|Described|p1174, p1175 Fig.1||Archean|Age: 2676+/-5 Ma. Overlies Kalgoorlie Group. Felsic volcanic-volcaniclastic and clastic sedimentary rocks. Deep marine sediments. Unconformably overlain by Merougil Group.||||||31-MAY-13
28372|Black Flag Group|60076|5|Briefly described|p12 Tb. 2, p19, p20|||Comprises upper felsic volcaniclastic and sedimentary rocks; and, lower dacites and andesites.  Unconformably overlain by Kurrawang Formation and Merougil beds.  Combined thickness: >6000m.  Geological Province: Ora Banda, Coolgardie and Kambalda domains.||||||09-OCT-12
28372|Black Flag Group|60514|4|Described|p26 Fig. 3, p29, p36 Fig. 6, |Archean|Archean|Includes; Morgans Island Epiclastic Fm, Newton Felsic Fm, Centenary Shale, Spargoville Fm, Pipeline Andesite, Triumph Gabbro, White Flag Fm. Conformably underlain by Paringa Basalt. . Age: 2666 - 2690 Ma.||||||09-OCT-12
28372|Black Flag Group|60555|5|Briefly described|p4 Tb. 1, p5, p10-11|Neoarchean|Neoarchean|Age: >2666Ma and see p6 Fig. 3. Deposition age. Thickness: >1000m (Morris, 1998). Felsic volcaniclastic and sedimentary succession, with subordinate extrusive and intrusive felsic and mafic rocks.||||||30-NOV-09
28372|Black Flag Group|60578|6|Mentioned|p6 Fig.1|Archean|Archean|||||||07-NOV-08
28372|Black Flag Group|60623|4|Described|p25 Fig.2|Archean|Archean|Unconformably overlies Paringa Basalt. Unconformably overlain by Merougil Formation. Geological Province: Eastern Goldfields.||||||07-NOV-08
28372|Black Flag Group|60626|5|Briefly described|p55|||Well bedded mudstone and fine-grained sandstones.||||||
28372|Black Flag Group|60627|5|Briefly described|p61, p65 Tb.1|||Sedimentary||||||
28372|Black Flag Group|61899|5|Briefly described|p118 Fig. 1|||Volcaniclastic sediments.||||||
28372|Black Flag Group|62083|5|Briefly described|p1005, p1014, p1016, p1019||Neoarchean|Yilgarn Craton. Eastern Goldfields Province. ~2665-2660 Ma andesitic volcanic and volcaniclastic rocks in lower part.|>2667 Ma; 2676 Ma|||Unconformably overlies Kambalda Group. Is unconformably overlain by Kurrawang Group. Golden Mile dolerite is emplaced near contact between Kambalda Group and Black Flag Group.|Tonalite-trondhjemite-granodiorite igneous rock provenance. Coarse clastic and epiclastic rocks. Andesitic volcanic and volcaniclastic rocks in lower part, and volcaniclastic and fine-grained clastic sedimentary rocks of upper part.|
28372|Black Flag Group|62093|6|Mentioned|p216 Tb. 1|||||||||
28372|Black Flag Group|62097|5|Briefly described|p305, p318|Archean|Archean|Felsic volcanic and voclaniclastic rocks; felsic units are intercalated with horizons of siltstone, mudstone and sandstone.  Includes mafic sills also. Geological Province: Kalgoorlie Terrane in Eastern Goldfields Superterrane of the Yilgarn Craton.||||||05-MAY-21
28372|Black Flag Group|62108|5|Briefly described|p1409 Tb. 1|Archean|Archean|Felsic, volcanic and sedimentary succession, upward coarsening. Age: 2676+/-4Ma. Thickness: >1km. Geol Prov: Yilgarn Craton (Boulder-Lefroy Shear Zone). See also p1410. See also Black Flag Beds. See also p1420.||||||07-FEB-11
28372|Black Flag Group|62109|5|Briefly described|p1428|||Black shales, greywackes and volcaniclastic rocks. Geological Province: Norseman-Wiluna fold belt/Yilgarn Craton.||||||
28372|Black Flag Group|62110|5|Briefly described|p1442 Fig. 1|Archean|Archean|Age: 2676+/-6Ma. Geological Province: Kambalda dome in the Norseman-Wiluna greenstone belt, Yilgarn Carton.||||||07-FEB-11
28372|Black Flag Group|62111|5|Briefly described|p1458 Figs. 1, 2|||Geological Province: Kambalda Dome in the Norseman-Wiluna greenstone belt of the Yilgarn Craton.||||||07-FEB-11
28372|Black Flag Group|63163|5|Briefly described|p76|||Overlies Golden Mile Dolerite. Geological Province: Kalgoorlie Terrane/Eastern Goldfields Province.||||||04-APR-07
28372|Black Flag Group|63463|6|Mentioned|p587|||Thick unit of volcanogenic sedimentary shales and sandstones.||||||
28372|Black Flag Group|63637|5|Briefly described|p3|||Geological province: Eastern Goldfields Province. Sedimentary unit with five principal lithofacies identified (details included on page 8 table 1.1).||||||17-OCT-07
28372|Black Flag Group|63981|5|Briefly described|p91, p93 Fig.3, |Archean|Archean|Comprises rocks assigned to Kalgoorlie and Kambalda Sequences.|||Includes Spargoville and White Flag Formations.||Felsic volcanic and volcaniclastic rocks.|
28372|Black Flag Group|64340|5|Briefly described|p7, p10, p22, p8 Tb. 1|Archean|Archean|Thickness: >1000m. Comprises felsic volcanic and volcaniclastic rocks with minor mafic units.||||||08-OCT-14
28372|Black Flag Group|64633|6|Mentioned|p8, p12.|||||Unit in Kalgoorlie sequence.||||
28372|Black Flag Group|64715|5|Briefly described|p1, p3, p5 Fig. 4|||Association of dominantly felsic volcanic and volcaniclastic rocks. See also p7 Fig. 7, p10.||||||16-DEC-08
28372|Black Flag Group|64771|5|Briefly described|p4|Neoarchaean|Neoarchaean|Swager et al. (1995). Southern Kalgoorlie Terrane.|2.69-2.66 Ga.||||A felsic volcaniclastic sequence.|
28372|Black Flag Group|64893|5|Briefly described|p30|Archaean|Archaean|Age range: c.2698 to c.2666Ma. Overlies the Kambalda sequence in the Kalgoorlie Terrane.||||||05-MAY-21
28372|Black Flag Group|65204|5|Briefly described|pg6 Tbl.1, p12, p13, p14, p15|Neoarchean||Upper part is intermediate rocks.|||Includes the Pipeline Andesite.|Intruded by Orinda Sill, Ora Banda Sill, Powder Sill; unconformably underlies Kurrawang Formation.|Rhyolite to andesite lava, tuff, volcanic breccia, felsic volcaniclastic sedimentary rocks ranging from coarse clastic sandstone to interbedded sandstone and siltstone; volcaniclastic conglomerate.|16-MAY-14
28372|Black Flag Group|65260|6|Mentioned|p6 Tb.1|Neoarchean||Youngest deposition age c. 2666 Ma.||||||
28372|Black Flag Group|65264|5|Briefly described|p9, p18, p19|||Unconformably overlain by Kurrawang Formation. These beds contain two unconformity-bound sequences - the Spargoville and Kalgoorlie sequences. Some lithological details for the Kalgoorlie terrane area.(p18). Geol.prov: Yerrida Basin. See also p20||||||07-FEB-11
28372|Black Flag Group|65834|5|Briefly described|p1, 7, 26, 33, 37-38, 53, 62|||Kalgoorlie Terrane.|2681 +/- 5 Ma (Nelson, pers. comm., 1994).||Pipeline Andesite; Orinda, Ora Banda, Powder Sills; Junction, Condenser, Golden Mile Dolerites; Triumph Gabbro; White Flag, Spargoville Formations.|Is correlated with Gindalbie Formation.|Felsic volcanic and sedimentary unit. Has an upper basalt unit in only the central domains.|
28372|Black Flag Group|66880|5|Briefly described|p7. |Archean|Archean|Four unconformity-bound sequences (the Kalgoorlie Sequence) of deposition in a series of transtensional deep-marine intra-arc basins.||||Unconformably overlies Kambalda Sequence. Is unconformably overlain by White Flag Formation.|A tonalite-trondhjemite-dacite sequence; dacitic (dominant), andesitic and rhyolitic volcaniclastic and epiclastic rocks with subordinate lavas.|
28372|Black Flag Group|67020|5|Briefly described|p660.|Archean|Archean|||||Overlies Paringa Basalt. Is unconformably overlain by Merougil Group.|Felsic volcanic and volcaniclastic rocks.|
28372|Black Flag Group|67198|5|Briefly described|p83 fig 42, p94 fig 45|||> 3000m thick. Kalgoorlie Terrane. In the St Ives Goldfield region major variations in age and provenance of Black Flag Group occur. See also references to Black Flag Formation (p5 Fig.2, p82).|c.2689 - >2658 Ma|Kalgoorlie Sequence||Overlies Paringa Basalt. It is disconformably overlain by Merougil Conglomerate|Clastic sedimentary rocks and felsic volcanic-volcaniclastic sequences.|11-SEP-17
28372|Black Flag Group|67269|5|Briefly described|p20-21 Fig.19|Neoarchean|Neoarchean|Kanowna, Eastern Goldfields. Contains un-named stromatolites with an axial zone; photograph shown to demonstrate the continuity of such zones through geological time, and to support the biogenic origin of stromatolitic structures in Strelley Pool Formation (East Pilbara Terrane).|2704 +/- 8 to 2676 +/- 5 Ma.|||||
28372|Black Flag Group|68109|6|Mentioned|p660|Neoarchean|Neoarchean||ca. 2690-2658 Ma|||Equivalent to Kalgoorlie Sequence.||08-OCT-14
28372|Black Flag Group|68217|6|Mentioned|p71|Precambrian|Precambrian|Used by Fairbridge (1953) to replace Black Flag Series, but no constituent units, so Black Flag Beds preferred here.||||||
28372|Black Flag Group|68289|4|Described|p6-p7, p6 fig 5, p11-p14|||Kalgoorlie Terrane. Deposition of this unit coincided with voluminous high Ca TTG granite magmatism in the Eastern Goldfields Superterrane. Interpreted by Krapez and Hand (2008) as Kalgoorlie Sequence. Unconformably overlies the mafic-ultramafic succession of the southern Kalgoorlie Terrane. Outcrop localities are provided in addition to local lithologies. See also p16-p17, p28-p29, p31-p32.|2690-2660 Ma|||Overlies the Paringa Basalt. Intruded by the Mungari Monzogranite.|Sedimentary rocks and mafic volcanics including extensive volcaniclastic rocks, rhyolitic to dacitic volcanics and extensive intrusive mafic complexes. Polymictic breccia, slate beds and felsic lavas are also present.|
28372|Black Flag Group|69152|5|Briefly described|geochron files |Neoarchean|Neoarchean|Interpreted time of emplacement of felsic volcanic breccia from this group: 2675+/-3 Ma.  From geochron file 100758.1.pdf, 1997?, age: 2681+/-5 Ma also for felsic volcanics, in 112110.1.pdf. See also 179684.1.pdf (2006) 177919.1.pdf, 177923.1.pdf (2007).||||||
28372|Black Flag Group|69181|5|Briefly described|p21|||Kalgoorlie Terrain, Yilgarn Craton.|||||Felsic to intermediate volcaniclastics.|
28372|Black Flag Group|69404|6|Mentioned|p4|Neoarchean|Neoarchean|Hosts economically important dolerite deposits.|c. 2690 - 2670 Ma||Golden Mile Dolerite|||
28372|Black Flag Group|69583|4|Described|p35, p39, p41|||Squire et al. (2010). Suggested tectonic settings briefly described. Equivalent to the Kalgoorlie Sequence of Krapez and Hand (2008). Over 3000m thick. Deposition was accompanied by widespread emplacement of a high-Ca TTG granite suite.|c.2690-2660 Ma (deposition).|||Unconformably overlies Paringa Basalt.|Extensive volcaniclastic rocks, rhyolitic to dacitic volcanic rocks, intrusive mafic complexes, and minor mafic volcanic rocks.|
28372|Black Flag Group|69631|5|Briefly described|p6-7, p11, p14-16, p18, p20-22, p26|Neoarchean|Neoarchean|See also p28-29, p52. Kalgoorlie Terrane. Tonalite-trondhjemite-granodiorite volcanism and associated sedimentary rocks and mafic intrusions. A rhyodacite from Morgans Island was dated at 2678 +/- 8 Ma (SHRIMP U-Pb zircon, Krapez et al., 2000).|c.2690-2660 Ma.|||Overlies Paringa Basalt. Is overlain by Navajo Sandstone (and Merougil Formation) unconformably.|Metasedimentary rocks including polymictic breccia, rare slate beds, and basal beds of oligomictic conglomerate. Extensive volcaniclastic rocks, rhyolitic to dacitic volcanic rocks, intrusive mafic complexes and minor mafic volcanic rocks.|
28372|Black Flag Group|70020|6|Mentioned|p120|||Geological province: Yilgarn Craton.||||||
28372|Black Flag Group|70087|6|Mentioned|p215|Archean|Archean||2670-2658 Ma.|||||
28372|Black Flag Group|70153|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Age derived from samples of felsic volcanic rock. An age of 2703 +/- 5 Ma from a quartzofeldspathic metasiltstone constrains deposition of its sedimentary protolith (177920.1.pdf, 177916.1.pdf).|2664 +/- 3 Ma (SHRIMP).||Includes Clianthus Flat Rhyodacite, Speedway Andesite, Centenary Shale.||Metamorphosed sandstone and siltstone, aluminosilicate schist, schist, shale, carbonaceous shale, conglomerate and mudstone, volcaniclastic sandstone and conglomerate; ferruginous chert, banded chert; andesite-basaltic andesite, dacite.|
28372|Black Flag Group|70276|6|Mentioned|p783|||Kalgoorlie terrane, Yilgarn Craton.|||Spargoville, Kalgoorlie Sequences.|||
28372|Black Flag Group|70326|5|Briefly described|p337,360|Neoarchean|Neoarchean|Geological province: Kambalda, Boorara, Coolgardie and Ora Banda domains, Kalgoorlie Terrane, Yilgarn Craton. Intruded by Condensor Dolerite and Golden Mile Diorite in the lower section.||||Correlable to Vivien Formation. Underlain by Paringa Basalt, and Grrenfields and Ora Banda sills.||
28372|Black Flag Group|70773|6|Mentioned|iv, p21, p24 fig 16, |||See also p25 fig 18, p26, p27 fig 22, p46.||||||
28372|Black Flag Group|70802|4|Described|179911.1.pdf|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Eastern Goldfields Superterrane, Yilgarn Craton. Sample GSWA 177911 (metasandstone) yielded a weighted mean 207Pb*/206Pb* date of 2684+\-40 Ma, interpreted as maximum depositional age of the sandstone protolith. Sample GSWA 177911 (metamorphosed felsic metavolcanic rock) yielded a weighted mean 207Pb*/206Pb* date of 2680+\-5 Ma, interpreted as igneous crystallisation age of the precursor felsic volcanic rock. Sample GSWA 177920 (granodiorite) yielded a weighted mean 207Pb*/206Pb* date of 2664+\-3 Ma, interpreted as igneous crystallisation/intrusion age of the monzogranite into Black Flag Group. Sample GSWA 177923 (metadacite) yielded a weighted mean 207Pb*/206Pb* date of 2677+\-3 Ma, interpreted as igneous crystallisation age of the volcanic protolith to the metadacite. Sample GSWA 179669 (volcaniclastic sandstone) yielded a weighted mean 207Pb*/206Pb* date of 2663+\-3 Ma, interpreted as igneous crystallisation age and maximum depositional age of the volcaniclastic sandstone. Sample GSWA 179684 (metarhyolitee) yielded an upper intercept age of 2679+\-9 Ma, interpreted as igneous crystallisation age of rhyolite.||||||
28372|Black Flag Group|70826|6|Mentioned|p9|Neoarchean|Neoarchean|Kalgoorlie Terrane.|||||Includes felsic volcanics|13-MAY-20
28372|Black Flag Group|70863|6|Mentioned|p9|||Kambalda Dome, Yilgarn Craton.||||||
28372|Black Flag Group|71148|6|Mentioned|p123, 130|Neoarchean|Neoarchean|Kalgoorlie Terrane, Yilgarn Craton.|2690-2670 Ma.|||||
28372|Black Flag Group|71166|5|Briefly described|p19, p118, p119 fig 3.89|||||||Overlies the Paringa Basalt.|Metasediments.|
28372|Black Flag Group|71168|6|Mentioned|p10|||||||||
28372|Black Flag Group|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma). Sample GSWA 112110 (carbonated sericitic feldspar-phyric quartzfeldpathic rock) yielded an interpreted emplacement age of 2681+\-5 Ma. Sample GSWA 177911 (fine-grained metasandstone) yielded a weighted mean 207Pb/206Pb date of 2684+\-40 Ma, interpreted to be maximum depositional age of the sandstone protolith. Sample GSWA 177919 (silicified, altered feldic metavolcanic rock) yielded a weighted mean 207Pb/206Pb date of 2680+\-5 Ma, interpreted to be crystallisation age of the precursor felsic volcanic rock. Sample GSWA 177920 (foliaed granodiorite intruding Black Flag Group) yielded a weighted mean 207Pb/206Pb date of 2664+\-3 Ma, interpreted to be crystallisation age of the intrusive granodiorite. Sample GSWA 177923 (metadacite) yielded a weighted mean 207Pb/206Pb date of 2677+\-3 Ma, interpreted to be crystallisation age of the precursor volcanic protolith. Sample GSWA 179669 (volcaniclastic sandstone; probably lateral continuation of Black Flag Group) yielded a weighted mean 207Pb/206Pb date of 2663+\-3 Ma, interpreted as the igneous crystallization age of the source rock, and is a maximum age for deposition of the volcaniclastic sandstone. Sample GSWA 179684 (metarhyolite) yielded a weighted mean 207Pb/206Pb date of 2676+\-9 Ma, interpreted as the igneous crystallization age of the rhyolite. Sample GSWA 204585 (metadacite) yielded a weighted mean 207Pb/206Pb date of 2671+\-1 Ma, interpreted as the igneous crystallization age of the dacite. Sample GSWA 211051 (porphyritic andesite) yielded a weighted mean 207Pb/206Pb date of 2690+\-7 Ma, interpreted as the magmatic crystallization age of the andesite. See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv. |2692-2655 Ma (inferred)||Includes Centenary Shale, Clianthus Flat Rhyodacite, Speedway Andesite.|Intruded by Depot Granodiorite.|Shale, carbonaceous shale, wacke, sandstone; metamorphosed, volcaniclastic; conglomerate; volcaniclastic, polymictic; andesite, basaltic andesite; dacite, feldspar-quartz porphyritic rock, aluminosilicate schist, kyanite/andalusite porphyroblasts.|
28372|Black Flag Group|72049|4|Described|p251, p253, p255-p256|||Referred to as the Early and Late Black Flag Group on p253 and p259. SHIRMP and LA-ICPMS analytical techniques and results are discussed in detail. A SHRIMP date pf 2683 +/- 4 Ma was derived from this study. See also p258-p261, p262-p263, p266-p272.|2686 +/- 3 Ma (Krapez et al., 2000)||Includes the Ballarat Turbidite, Golden Valley Conglomerate, Mount Kirk Formation, and the Grave Dam Grit.|Overlies the Kambalda Sequence. Intruded by the Golden Mile Dolerite.|Feldspar-rich pyroclastic debris and coarse mafic conglomerate. Framework-supported feldspar-rich granule breccia intercalated with medium- to coarse-grained volcanic sandstone; mudstone is very rare.|05-MAY-21
28372|Black Flag Group|72057|5|Briefly described|p237-238,242,244,247|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton. Also referred to as Kalgoorlie Sequence. Includes dolerites in the early section, and intercalated sandstone and coarse mafic breccias in the late section.|c. 2690-2660 Ma||Includes Condensor, Golden Mile, Junction and Cave Rocks dolerites.|Overlain by Merougil Group. Underlain conformably to unconformably  by Kambalda Sequence. Equivalent to Vivien Group.||
28372|Black Flag Group|72095|4|Described|p3 Fig 2,4,5, 6,8,9, 10-25|Neoarchean|Neoarchean|Eastern Goldfields, Yilgarn Craton. Extensively intruded by mafic and ultramafic sills. Previously interpreted to contain rocks with Intermediate-Th Basalt (ITB; Barnes et al., 2012) geochemistry, but have since been reassigned to Devon Consols Basalt (this study). Detailed geochemistry is described.|2692-2665 Ma|||Underlain unconformably or disconformably by Hannans Subgroup. Overlies Paringa Basalt? Or volcanic equivalent of Eureka Dolerite?|Felsic and mafic volcanic and volcaniclastic rocks.|
28372|Black Flag Group|72252|5|Briefly described|p11|||St. Ives Au-Ni camp, Kambalda Domain, Yilgarn Craton. 1500m thick. Appears mis-spelt as Black Flags Group.|||||Argillite, wacke, felsic and intermediate intrusive rocks, volcanic conglomerate, breccia and tuff.|
28372|Black Flag Group|73151|6|Mentioned|p14|||||||Equivalent to the Vivien Formation and Scotty Creek Formation.|Includes conglomerates with clasts commonly derived from supracrustal volcanic and high level subvolcanic intrusive sources.|
28372|Black Flag Group|73238|5|Briefly described|p18||||2690-2670 Ma.|||Overlies the Kambalda Sequence.|Deep marine siliciclastic turbiditic wacke and mudstone, and localised andesite-dacite volcanics and volcaniclastic sedimentary rocks.|
28372|Black Flag Group|73300|6|Mentioned|p1112-1113|Neoarchean|Neoarchean|Yilgarn Craton, Kalgoorlie terrane.|2674 +/- 6 Ma|Kalgoorlie Sequence||Overlies the Kambalda Sequence, Paringa Basalt.|Sedimentary and volcanic units.|
28372|Black Flag Group|73391|4|Described|vii, 19-20, 22, 25, 38-39, 50, 68, 102|||See also p108-109, 114, 121, 131, 142, 167, 182, 186, 197, 217, 230, 233, 235-236, 242-243, 248, 252, 349, 419, 421, Appendices. Swager et al. (1990). The entire Formation is variably exposed for ~45km S of the contact with White Flag Formation. Stratigraphy differs from that of Krapez et al. (2000). Subdivided into seven depositional and magmatic sequences. Lithologies vary in different Domains. Probably over 3000m thick. See Black Flag Formation.|2676 +/- 5 Ma.||Spargoville Formation, White Flag Formation, Black Flag Formation.|Is overlain unconformably by Kurrawang Formation.|Andesite, quartz porphyry, volcanogenic sedimentary rocks, shale, dacitic volcanic rocks, feldspathic grit, feldspar porphyry; (upper part) porphyry conglomerate.|
28372|Black Flag Group|73453|6|Mentioned|p16|||Kalgoorlie-Kurnalpi terrane. Hosts 2.66-2.64 Ga gold mineralisation.||||||
28372|Black Flag Group|73596|5|Briefly described|p1159, 1162|Neoarchean|Neoarchean|Squire et al. (2010). Kalgoorlie-Kambalda area, Kalgoorlie Terrane.|c.2690-2660 Ma.||Talbot, White Flag, Gibson-Honman, Gidji Lake Formations.|Overlies Hannans, Coolgardie, Broad Arrow Subgroups. Is overlain by Merougil, Panglo Formations.||
68511|Black Hill Well Monzogranite|63441|2|Defined|p46 Appx.1, p10 Tb. 2|Archean|Archean|Of Orpheus Supersuite. Age:crystallisation age of 3018+/-19Ma; later, leucocratic veining during a 2970+/-5 magmatic event. Geol. province: Pilbara Craton. Intrudes Ruth Well Fm Roeburne Gp) + Andover Intrusion. Weakly foliated monzogranite.See also p37.||||||07-FEB-11
68511|Black Hill Well Monzogranite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Orpheus Supersuite. Geological province: Pilbara Craton. Weakly foliated monzogranite.||||||07-NOV-08
68511|Black Hill Well Monzogranite|64580|4|Described|map legend||Mesoarchean|Of Orpheus Supersuite. Weakly foliated monzogranite.||||||15-DEC-08
68511|Black Hill Well Monzogranite|67201|4|Described|p16-17 Fig.9|Archean|Archean|Pilbara Craton. In Roebourne-Karratha area.||Orpheus Supersuite|||Weakly foliated monzogranite.|
68511|Black Hill Well Monzogranite|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Orpheus Supersuite.|||Weakly foliated monzogranite|
68511|Black Hill Well Monzogranite|70775|5|Briefly described|p15, p46, p58|||Pilbara Craton. Mis-spelt as the Black Hill Monzogranite on p49. This is the largest intrusion of the Orpheus Supersuite.|~3018 Ma|Orpheus Supersuite|||Weakly foliated monzogranite.|05-FEB-18
68511|Black Hill Well Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
68511|Black Hill Well Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|De Grey Superbasin.|3018+/-19 Ma|Orpheus Supersuite|||Weakly foliated monzogranite; leucocratic veins; metamorphosed.|
29567|Black Rabbit Member|42989|3|Fully described|p21|||of Missouri Basalt||||||
29567|Black Rabbit Member|43101|3|Fully described|p47|||of Missouri Basalt||||||
30673|Black Rock Granodiorite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1860Ma. Geological province: Kimberley Province (West).||||||07-FEB-11
30673|Black Rock Granodiorite|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|Approx 1865 - 1850 Ma.||||||
30673|Black Rock Granodiorite|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite. Biotite-hornblende granodiorite and tonalite. Age: c. 1865-1850Ma. In the Hooper Complex and Lamboo Complex western zone.||||||07-NOV-08
30673|Black Rock Granodiorite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Paperbark Supersuite.||||||07-NOV-08
30673|Black Rock Granodiorite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Paperbark Supersuite.|||Biotite-hornblende granodiorite and tonalite.|
30673|Black Rock Granodiorite|72437|5|Briefly described|p77|||Hooper Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Granodiorite and microdiorite.|
35661|Black Swan Komatiite|23131|6|Mentioned|p340|||||||||04-MAR-16
24731|Blackstone Range Gabbro|24496|5|Briefly described|p15|Mesoproterozoic|Mesoproterozoic|Age: ~1080 Ma. Emplaced along unconformity between Bentley Supergroup and underlying crystalline basement.  Geological Province: Musgrave Block.||||||
24731|Blackstone Range Gabbro|30386|5|Briefly described|p14|||||||||
24731|Blackstone Range Gabbro|30389|6|Mentioned|p13|||See also P15||||||
24731|Blackstone Range Gabbro|30390|4|Described|p129|||See also P130-138||||||
24731|Blackstone Range Gabbro|32692|6|Mentioned|p186|||Unit cell dimensions of olivines||||||
24731|Blackstone Range Gabbro|35726|6|Mentioned|p102|||See also P103||||||
24731|Blackstone Range Gabbro|36886|3|Fully described|p202|||||||||
24731|Blackstone Range Gabbro|43052|6|Mentioned|p162|||||||||
24731|Blackstone Range Gabbro|44139|5|Briefly described|p284, p285 Fig. 3-69|||Of Giles Complex. 3350m sequence of troctolite, norite, gabbro.| | ||||10-SEP-12
24731|Blackstone Range Gabbro|50607|6|Mentioned|p3.3|||Geological Province: Musgrave Block.||||||
24731|Blackstone Range Gabbro|61341|5|Briefly described|Map legend|||Presented in the compound name Blackstone Range Troctolite/Gabbro. Intrusion.||||||21-SEP-05
77450|Blacktip Member|67354|4|Described|p74, p78 Fig.7A, pp82-83, p91, p107.|Sakmarian|Sakmarian|Informal name for the upper part of the Kuriyippi Formation, which this author says needs redefining; he includes it in the Treachery Formation. Several cores display heterolithic facies; rapid, high energy deposition with de-watered sandstones and boulder conglomerates. The palynology is discussed in detail. May be equivalent to the Hoya Formation.||Unit in Treachery Formation.||||31-OCT-12
82996|Blacktop kimberlite|75075|6|Mentioned|p419, p420 Fig.1|||Western Pilbara Craton. [Appears in formal capitalisation as Blacktop Kimberlite].|||||Diamondiferous.|
25793|Blina Shale|7433|5|Briefly described|p25 Fig.2, pp40-41, pp52-53.|||Gregory and southeast Fitzroy Sub-basins, Canning Basin. Mudflats and fringing swamps. Contains vertebrate bones, and acritarchs and marine macrofossils. Mudcracks common, but absence of evaporites implies high water table and humid environment.||||Is overlain by Erskine Sandstone.|Thinly-bedded, bioturbated mudstone.|
25793|Blina Shale|13242|6|Mentioned|p225|Early Triassic|Early Triassic|Contemporaneous with deposition of Lower Mount Goodwin Formation in the Bonaparte Basin. Geological Province: Canning Basin.||||||07-FEB-11
25793|Blina Shale|13255|6|Mentioned|p376|Triassic|Permian|Marine sediments. Mentioned only as 'the Chirup and Blina Shales'.||||||
25793|Blina Shale|13354|6|Mentioned|p376 Fig.7.|Early Triassic|Early Triassic|Onshore Canning Basin. Overlies Millyit Sandstone and underlies Erskine Sandstone.||82||||28-OCT-14
25793|Blina Shale|14227|5|Briefly described|p10|Triassic|Triassic|Geological Province: Canning Basin.||||||07-FEB-11
25793|Blina Shale|22718|5|Briefly described|P5, Table1 P6||Early Triassic|||||||
25793|Blina Shale|22741|5|Briefly described|P29, Table3 P11||Early Triassic|||||||
25793|Blina Shale|22753|5|Briefly described|Fig.3 p585|Triassic|Triassic|||||||
25793|Blina Shale|22764|4|Described|Table 2 p9||Early Triassic|Thickness: 130 m. Disconformable on Millyit Sandstone, conformable beneath Erskine Sandstone.||||||01-FEB-10
25793|Blina Shale|22767|5|Briefly described|Table3 P14, P22||Early Triassic|||||||
25793|Blina Shale|22776|4|Described|Table.3|Early Triassic|Early Triassic|||||||
25793|Blina Shale|22814|5|Briefly described|fig2|Triassic|Triassic|||||||
25793|Blina Shale|23722|6|Mentioned|p35|Triassic|Triassic|||||||
25793|Blina Shale|23765|5|Briefly described|Map Legend|Triassic|Triassic|||||||
25793|Blina Shale|23766|4|Described|p14 Tb. 2|Triassic|Triassic|Consists of mainly dark-grey shale and siltstone with minor sandy claystone and fine sandstone. Thickness: 462m.  See also p22.||||||13-NOV-07
25793|Blina Shale|24061|5|Briefly described|p182|Triassic|Triassic|Geological Province:  Canning Basin. Maximum thickness: 310m.||||||
25793|Blina Shale|24062|5|Briefly described|p186 Table 1|Triassic|Triassic|Geological Province: Canning Basin.||||||
25793|Blina Shale|24160|6|Mentioned|p45|Triassic|Triassic||||||Mudstones.|
25793|Blina Shale|24466|5|Briefly described|p368 Fig. 3|Triassic|Permian|||||||
25793|Blina Shale|29633|4|Described|p435|||||||||
25793|Blina Shale|29817|6|Mentioned|p13|||Permian||||||
25793|Blina Shale|30110|6|Mentioned|p81|||Triassic.||||||
25793|Blina Shale|30186|6|Mentioned|p104|||Crustaceans occurrence||||||
25793|Blina Shale|30286|6|Mentioned|p1094|||Lower Triassic age||||||
25793|Blina Shale|30287|6|Mentioned|p5|||Lower Triassic||||||
25793|Blina Shale|30466|6|Mentioned|p5|||Lower Triassic age||||||
25793|Blina Shale|30525|6|Mentioned|Map legend|Triassic|Triassic|||||||
25793|Blina Shale|30533|4|Described|p27|||See also Table 8.||||||13-NOV-07
25793|Blina Shale|30547|6|Mentioned|p426|||Correlation||||||
25793|Blina Shale|30550|6|Mentioned|p82|||Lower Triassic age||||||
25793|Blina Shale|30565|6|Mentioned|p116|||||||||
25793|Blina Shale|30897|6|Mentioned|p19|||Subsurface unit||||||
25793|Blina Shale|31396|6|Mentioned|p1183|||||||||
25793|Blina Shale|32163|6|Mentioned|p282|||Refers Balme (1969)||||||
25793|Blina Shale|32648|6|Mentioned|p32|||L.Triassic||||||
25793|Blina Shale|32710|6|Mentioned|p116|||||||||
25793|Blina Shale|32979|6|Mentioned|p38|||Correlation with basins in India||||||
25793|Blina Shale|33406|6|Mentioned|p100|||Correlation of fossils.||||||
25793|Blina Shale|33627|6|Mentioned|p582|||||||||
25793|Blina Shale|34008|3|Fully described|p68|||See also pp67,69,70,75. Lower Triassic.||||||13-NOV-07
25793|Blina Shale|34009|6|Mentioned|Table III|||L.Triassic||||||
25793|Blina Shale|34010|6|Mentioned|Cor. chart|||L.Triassic||||||
25793|Blina Shale|34113|6|Mentioned|p65|||Brachiopods||||||
25793|Blina Shale|34172|6|Mentioned|p57|||||||||
25793|Blina Shale|34274|6|Mentioned|p117|||L.Triassic||||||
25793|Blina Shale|34287|6|Mentioned|p151|||Triassic. See also p162.||||||17-JUL-20
25793|Blina Shale|34532|6|Mentioned|p222|||See also p225. L.Trias.||||||04-NOV-15
25793|Blina Shale|35120|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
25793|Blina Shale|35124|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
25793|Blina Shale|35205|6|Mentioned|Map legend|Triassic|Triassic|||||||
25793|Blina Shale|35236|6|Mentioned|p8|||||||||
25793|Blina Shale|35275|6|Mentioned|Fig.5|||||||||
25793|Blina Shale|35280|6|Mentioned|p148|||||||||
25793|Blina Shale|35901|6|Mentioned|p16|||||||||
25793|Blina Shale|35913|6|Mentioned|p37|||||||||
25793|Blina Shale|35914|4|Described|p9|||||||||
25793|Blina Shale|35915|6|Mentioned|p25|||||||||
25793|Blina Shale|36121|6|Mentioned|p32|||||||||
25793|Blina Shale|36224|5|Briefly described|Map legend|Early Triassic|Early Triassic|Mudstone, sandy mudstone, lamintaed to thin bedded;minor fine sandstone; fossiliferous.||||||01-FEB-05
25793|Blina Shale|36225|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
25793|Blina Shale|36257|6|Mentioned|Table 2.1|||||||||
25793|Blina Shale|36634|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
25793|Blina Shale|36890|3|Fully described|p345|||||||||
25793|Blina Shale|37106|6|Mentioned|p277|||||||||
25793|Blina Shale|37368|6|Mentioned|Map legend|Triassic|Triassic|||||||
25793|Blina Shale|38375|6|Mentioned|p547|||||||||
25793|Blina Shale|38444|6|Mentioned|p300|||||||||
25793|Blina Shale|38878|6|Mentioned|Map legend|Middle Triassic|Early Triassic|Early - Middle Triassic.||||||17-JUL-20
25793|Blina Shale|38886|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
25793|Blina Shale|39059|6|Mentioned|p590|||||||||
25793|Blina Shale|39796|6|Mentioned|Map legend|Triassic|Triassic|||||||
25793|Blina Shale|39922|6|Mentioned|p362|||||||||
25793|Blina Shale|40045|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
25793|Blina Shale|40633|6|Mentioned|p11|||||||||
25793|Blina Shale|40838|6|Mentioned|p281|||||||||
25793|Blina Shale|40992|6|Mentioned|Fig.11|||||||||
25793|Blina Shale|40999|6|Mentioned|p307|||||||||
25793|Blina Shale|41056|6|Mentioned|p22|||||||||
25793|Blina Shale|41101|6|Mentioned|p292|||||||||
25793|Blina Shale|41158|5|Briefly described|p199|||Mention p156.||||||17-JUL-20
25793|Blina Shale|41169|6|Mentioned|p148|||See also Fig.3||||||
25793|Blina Shale|41215|6|Mentioned|p281|||||||||
25793|Blina Shale|41436|6|Mentioned|p43|||||||||
25793|Blina Shale|41438|6|Mentioned|p106|||||||||
25793|Blina Shale|41449|5|Briefly described|p256|||||||||
25793|Blina Shale|41688|4|Described|p13|||||||||
25793|Blina Shale|41730|6|Mentioned|Fig.3|||||||||
25793|Blina Shale|41732|6|Mentioned|p534|||||||||
25793|Blina Shale|42473|6|Mentioned|p91|||||||||
25793|Blina Shale|42477|5|Briefly described|p132|||||||||
25793|Blina Shale|42571|5|Briefly described|p20, Table1 p9|||||||||
25793|Blina Shale|42710|5|Briefly described|map legend|Triassic||||||||
25793|Blina Shale|42811|5|Briefly described|p45|||||||||
25793|Blina Shale|42814|5|Briefly described|p23|||||||||
25793|Blina Shale|42930|5|Briefly described|Fig.1 p473|Early Triassic|Late Permian|Unconformably overlies Liveringa Formation; unconformably underlies Erskine Sandstone. Geological Province: Canning Basin. Marine deposits.||||||13-NOV-07
25793|Blina Shale|43173|6|Mentioned|12,54||Early Triassic|||||||
25793|Blina Shale|43281|5|Briefly described|Map legend||Triassic|||||||
25793|Blina Shale|43563|6|Mentioned|Fig.2,p5||Scythian|||||||
25793|Blina Shale|43656|6|Mentioned|Fig.2,p8|Scythian|Scythian|||||||
25793|Blina Shale|43666|6|Mentioned|p28,45 Table 2||Permian|||||||
25793|Blina Shale|43746|6|Mentioned|Fig.2,p11|Scythian|Scythian|||||||
25793|Blina Shale|43818|6|Mentioned|Fig.2.p39|Early Triassic|Late Permian|||||||
25793|Blina Shale|43932|4|Described|p10,Tb.1 p5|Anisian|Scythian|||||||
25793|Blina Shale|43976|5|Briefly described|p69,71|||||||||
25793|Blina Shale|44006|14|Not recorded|p65-66,68,82,88|||New amphibian, Deltasaurus gen.nov.; W.Kimberleys||||||
25793|Blina Shale|44040|14|Not recorded|p43|||||||||
25793|Blina Shale|44143|4|Described|p.434 Table 4-19, p447-448|Triassic|Triassic|Up to 500m thick; mudstone,shallow marine. Passes laterally into and conformably overlies Millyit Sandstone; disconformably overlies Chirup Formation and Liveringa Group. Lateral equivalent of Locker Shale. Type section at Erskine Range (DERBY: 17deg 51' 25" S, 124deg 21' 40" E). ||||||22-NOV-17
25793|Blina Shale|44237|14|Not recorded|p.213|||||||||
25793|Blina Shale|44403|2|Defined|p.4,8,9,10|||E/51-12, top eroded, unconformable above Liveringa Formation.Type section: Playford & others ( 1975) have suggested?a section that McKenzie (1961) measured in the Erskine Range (17degrees 51 '25"S, 124degrees21'40"E), which we regard as the type section herein (61 in Table 6). Lithology in Blackstone 1: 9-280m  -. Siltstone: grey to whitish, finely micaceous, pyritic; finely interbedded with shale: grey and green; and minor sandstone: grey, fine-grained. Traces of glauconitic and calcareous material occur in the lower part. 280-320 m - Siltstone: glauconitic, micaceous, and pyritic, with minor sandstone interbeds.||||||14-DEC-22
25793|Blina Shale|44404|14|Not recorded|map legend||Triassic|||||||
25793|Blina Shale|44994|6|Mentioned|Fig.7|||Correlation. Triassic.||||||
25793|Blina Shale|44998|2|Defined|p.108-116|||Underlain [?] by Culvida Sandstone, Liveringa Formation. Overlain by Erskine Sandstone. See also p69,88,103-4,135,173,-8,212,229,231,245,map, App.6 p294.||||||17-JUL-20
25793|Blina Shale|45022|14|Not recorded|p105||Triassic|||||||
25793|Blina Shale|45153|2|Defined|App.5-86|Middle Triassic|Middle Triassic|Previously named Belina Shale, Wongal Shale and Wonjil Shale.||||||13-NOV-07
25793|Blina Shale|45156|6|Mentioned|p31|||Correlative||||||
25793|Blina Shale|45158|3|Fully described|p16|||||||||
25793|Blina Shale|46849|6|Mentioned|Fig. 5|||||||||
25793|Blina Shale|46863|6|Mentioned|p25|||||||||
25793|Blina Shale|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
25793|Blina Shale|48573|2|Defined|p.3,8-10|||(E51-7/Alexander Creek)||||||
25793|Blina Shale|48826|14|Not recorded|p.30|||Tb.III. p.23,28,30,37. Pl.I. Overlies Noonkanbah Formation. Correlates with Erskine Sandstone. (E52-13,F52-1).||||||
25793|Blina Shale|48857|14|Not recorded|p.13,14|||||||||
25793|Blina Shale|60386|6|Mentioned|p297, 300|Early Triassic|Early Triassic|Roebuck/Canning Basin/Browse Basin. Distal shelf/basin.||||||
25793|Blina Shale|61021|5|Briefly described|p36 Fig. 2|Scythian|Tatarian|Geological Province: Canning Basin.||||||17-DEC-07
25793|Blina Shale|62921|6|Mentioned|p877|Early Triassic|Early Triassic|Canning Basin. Contains stereospondyls (Tetrapoda, Temnospondyli).||||||
25793|Blina Shale|63172|6|Mentioned|p321|||Contains amphibian faunas.||||||07-FEB-11
25793|Blina Shale|63929|6|Mentioned|p131 Fig.2.|Early Triassic|Early Triassic|Onshore Canning Basin. Primarily marine sediments.||||Overlies Millyit Sandstone. Is overlain by Erskine Sandstone.||
25793|Blina Shale|64187|5|Briefly described|p320 Fig. 2|Early Triassic|Early Triassic|Underlain unconformably by Liveringa Group, overlain by Erskine Sandstone. Shale, siltstone, sandstone (marginal marine). Geological Province: Canning Basin.||||||03-FEB-10
25793|Blina Shale|64580|4|Described|map legend|Early Triassic|Early Triassic|Eastern Canning Basin. Siltstone and shale; minor phosphatic horizons.||||||09-DEC-08
25793|Blina Shale|64643|5|Briefly described|p9, p3 Fig. 2|Lower Triassic|Lower Triassic|Up to 410m of fossiliferous mudstone and fine-grained sandstone. Type section in Erskine Range.||||||24-NOV-08
25793|Blina Shale|64981|6|Mentioned|p669 Fig.3.|Scythian|Scythian|||||Overlies Liveringa Formation. Is overlain by Erskine Sandstone.||
25793|Blina Shale|65301|5|Briefly described|p5 Fig. 4|Early Triassic|Early Triassic|Geological province: Canning Basin.||||||
25793|Blina Shale|65449|6|Mentioned|p6|Early Triassic|Early Triassic|||||Overlies Millyit Sandstone. Is overlain by Erskine Sandstone.||
25793|Blina Shale|66124|5|Briefly described|p169, p170 Fig.2|Olenekian|Induan|Canning Basin. Marine; contains conodonts. Thickness greater than 300m in places. Overlies Millyit Sandstone, underlies Erskine Sandstone. Conodonts have been recovered from the Blina Shale in Blackstone 1 and Langoora 1, but the limited fauna is not age-diagnostic .||||||08-OCT-20
25793|Blina Shale|66949|4|Described|p4 Fig.2, p7, p26-27, p31, p46-47 Appx.2|Early Triassic|Early Triassic|See also p55 Appx.3, p60-65 Appx.4; p76,79,83,85-86,90-91 Appx.5; Plates 2-4,6,10. Defined by Brunnschweiler (1954) citing Reeves (1951) as originator of the name [which he in fact spelt Belina]: see also Belina Shale (p24). Type section detailed. Up to 500m thick (p26 says 410m, 403m and 401m); shallow marine deposits. Fossils include vertebrates, conchostracans, plant remains, brachiopods and abundant microplankton, foraminifera. Biostratigraphic zonation.  Unlikely hydrocarbon source or seal. Available core and Formation picks detailed.||||Disconformably overlies Chirup Formation and Liveringa Group. Passes laterally into, and conformably overlies, Millyit Sandstone.|Fossiliferous mudstone and fine-grained sandstone.|04-NOV-15
25793|Blina Shale|67202|6|Mentioned|p44 Fig.2.10|||Canning Basin. An aquiclude.||||||
25793|Blina Shale|68007|6|Mentioned|p4|Early Triassic|Early Triassic|Canning Basin.||||||25-FEB-20
25793|Blina Shale|68656|6|Mentioned|GEOL_LUT_CSV/500k_geologyp08_lut|Early Triassic|Early Triassic||||||Siltstone and shale; minor phosphatic horizons.|
25793|Blina Shale|68811|6|Mentioned|p81|Triassic|Triassic|||||Overlain by the Erskine Sandstone.||15-APR-20
25793|Blina Shale|68902|5|Briefly described|p9 fig 5, p10|Triassic|Triassic|Only a 25m-thick interval attributed to this unit was encountered in BMR 4A Mandora in the Waukarlycarly Embayment, and even that section's age is possibly Cretaceous.||||Disconformably overlies Millyit Sandstone, overlain by Erskine Sandstone.||
25793|Blina Shale|69029|5|Briefly described|p319,321|Olenekian|Induan|Of Canning Basin. Acts as seal to Grant Group reservoirs in the Boundary, Sundown, and West Terrace oilfields on the Lennard Shelf.||||Overlain by Wallal Sandstone. Underlain by Liverina Group.||
25793|Blina Shale|69099|5|Briefly described|500k_geologyp08_lut.csv|Early Triassic|Early Triassic||||||Siltstone and shale; minor phosphatic horizons.|30-JUL-15
25793|Blina Shale|69182|6|Mentioned|Ch4 p3, Ch4 p9, Ch4 p15-p16|Lower Triassic|Lopingian|Canning Basin. Contains local to regional seals. See also  Ch4 p30-p35, Ch4 p43, Ch4 p45, Ch4 p47, Ch4 p50-p58, Ch4 p63, Ch4 p74-p77, Ch4 p83-p84, Ch4 p88, Ch4 p90. ||||Conformably overlies the Millyit Sandstone. Overlain by the Erskine Sandstone.||
25793|Blina Shale|69297|6|Mentioned|p351|Early Triassic|Permian|Canning Basin. ||||||
25793|Blina Shale|69312|5|Briefly described|p3, p23 fig 27, p26 fig 33|Anisian|Olenekian|Canning Basin. ||||Overlies the Liveringa Group. Faulted against the Wallal Sandstone [?].|Shale, carbonate shales, marl.|11-FEB-20
25793|Blina Shale|69587|5|Briefly described|500k_geologyp08_lut.csv|Early Triassic|Early Triassic||||||Siltstone and shale; minor phosphatic horizons|
25793|Blina Shale|69634|5|Briefly described|500k_geologyp08_lut.csv|Early Triassic|Early Triassic||||||Siltstone and shale; minor phosphatic horizons|
25793|Blina Shale|70154|4|Described|500k_interpgeop14_lut.csv|Lower Triassic|Lower Triassic||247-252 Ma||||Siltstone and shale, minor phosphatic horizons|
25793|Blina Shale|70774|5|Briefly described|p4, p9|Early Triassic|Early Triassic|Fitzroy Trough, Lennard Shelf and Willara and Kidson Sub-basins, Canning Basin.||||Overlies the Millyit Sandstone. Overlain by the Erskine Sandstone.||10-FEB-20
25793|Blina Shale|70826|6|Mentioned|p7 tbl 4|Triassic|Triassic|Canning Basin.||||||
25793|Blina Shale|70878|5|Briefly described|p722 Fig.17|Triassic|Triassic|Fitzroy Trough, NW Canning Basin.||||||
25793|Blina Shale|71146|5|Briefly described|p6, p12 fig 8|Early Triassic|Lopingian|Canning Basin.||||Overlies the Millyit Sandstone. Overlain by the Erskine Sandstone.|Shale.|
25793|Blina Shale|71267|4|Described|GEOL_LUT_CSV files|Lower Triassic|Induan|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|252.17-247.2 Ma (biostrat)||||Shallow marine to freshwater, fossiliferous and commonly bioturbated well-bedded siltstone with common small-scale cross beds, shale, and very fine sandstone, mudstone.|14-DEC-22
25793|Blina Shale|71623|5|Briefly described|p345 fig 2|Scythian|Scythian|Canning Basin. Hosts Macrofossils.||||Unconformably overlies the Millyit Sandstone.||
25793|Blina Shale|71894|5|Briefly described|p4|Middle Triassic|Lower Triassic|Canning Basin.||||Overlies the Millyit sandstone. Unconformably overlies the Lightjack Formation. Overlain by the Erskine Sandstone.|Shale.|
25793|Blina Shale|72034|5|Briefly described|500k_interpgeop16_lut|Early Triassic|Induan|Canning Basin.  Age from biostratigraphy.|||||Siltstone and shale; minor phosphatic horizons.|
25793|Blina Shale|72497|5|Briefly described|p3 Fig.2.|Induan|Induan|Shown as occuring in the Anketell, Tabletop, Ryan Shelves, Willara and Kidson Sub-basins. Also shown as occuring in the Fitzroy Trough, Betty and Balgo Terraces and part of the Lennard Shelf and Margaret Terrace. Age shown as early Scythian ~=Induan.||||Conformably underlies Erskine and Culvida Sandstone. Unconformably underlies Wallal Sandstone. Unconformably overlies Liveringa Group.||
25793|Blina Shale|72499|4|Described|p7 Fig.6, p54, p95.|Early Triassic|Lopingian|Located in the Willara Sub-basin and Fitzroy Trough. Identified at the top of the Sundown 3 well log.||||Overlies Millyit Sandstone and underlies Erskine Sandstone. Shown as unconformably overlying Noonkanbah Formation.||
25793|Blina Shale|72505|5|Briefly described|p890|Induan|Induan|Canning Basin.||||Shown as equivalent to Penguin Formation.Partial equivalent to Locker Shale, Kockatea Shale.||
25793|Blina Shale|73117|5|Briefly described|p3, p109, p116, p123-124, p135, p137|Lower Triassic|Lower Triassic|Canning Basin.||||Underlain by Millyit Sandstone. Overlain by Erskine Sandstone.|Dominantly shale and mudstone.|
25793|Blina Shale|73304|6|Mentioned|p71, p77|||Canning Basin. Permian-Triassic (late Changhsingian) mass extinction level occurs at the lower boundary.||||Underlain by Hardman Formation.||
25793|Blina Shale|73445|5|Briefly described|p3, 6, 8, 12, 24, 65-118|||Canning Basin. 90m thick.||||Overlies Millyit Sandstone transitionally. Is overlain by Erskine Sandstone.|Mainly siltstone, claystone and fine-grained sandstone; minor phosphatic horizons.|
36765|Bloods Range Formation|50286|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group.||||||
36765|Bloods Range Formation|50321|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group.||||||28-MAY-04
36765|Bloods Range Formation|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group.  Red shales, polymictic conglomerate, volcaniclastics, tuffaceous horizons and local lensoidal quartz sandstone beds.  Geological Province: Musgrave Block.||||||
36765|Bloods Range Formation|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Schist, schistose quartz conglomerate. Of Tjauwata Group. Geological Province: Musgrave Block.||||||14-JAN-05
36765|Bloods Range Formation|61154|5|Briefly described|p16, p18 Fig. 10|Mesoproterozoic|Mesoproterozoic|Of Tjauwata Group. Clastic red-beds of polymictic conglomerate, fine sst and siltstone, grading upwards to immature sst; tuffaceous layers and local lensoidal quarts sst beds. Transitional over Puntitjata Rhyolite. Geol. Prov: Musgrave Block.||||||18-JUL-05
36765|Bloods Range Formation|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group.  Red shales, polymictic conglomerate, volcaniclastics, tuffaceous horizons and local lensoidal quartz sandstone.||||||19-OCT-05
36765|Bloods Range Formation|62989|5|Briefly described|p39|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. Disconformably overlain by Kulail Sandstone in base of Amadeus Basin. Succession of redbed sediments, volcaniclastic rocks and interlayered fine sandstone, siltstone and clast-supported pebble conglomerate; alluvial/fluvial setting.||||||25-JAN-10
36765|Bloods Range Formation|64580|4|Described|map legend||Mesoproterozoic|Of Tjauwata Group. Metamorphosed sandstone and siltstone, and felsic and mafic schist derived from volcanic rock.||||||15-DEC-08
36765|Bloods Range Formation|65233|5|Briefly described|p2|||Overlies Mount Harris Basalt. Geological province: Amadeus Basin. Comprises red beds, volcaniclastic rocks and fine-grained to conglomeratic clastic rocks.||||||07-FEB-11
36765|Bloods Range Formation|65256|1|Redefined|p39-40, p6 Tb.1, p8, 10, 12, 14-15, 37|Neoproterozoic|Stenian|Variation of published name: formerly Bloods Range Beds and Bloods Range beds. Thickness approx 100m (laterally variable). No longer correlated with Dixon Range beds. Appears to be derived from Puntitjata Rhyolite and Mount Harris Basalt.||Uppermost unit of the Tjauwata Group|Includes Wankari volcanics.|Overlies Mount Harris Basalt and Puntitjata Rhyolite; unconformably underlies Kulail Sandstone/Dean Quartzite; intruded by Walu Granite.|Polymictic pebble conglomerate, quartzite-cobble conglomerate, immature sandstone, red and dark purple fine sandstone and siltstone, epiclastic and volcaniclastic rocks, rare tuff.|24-MAR-15
36765|Bloods Range Formation|69091|6|Mentioned|p103 Fig.5.6|||||||||
36765|Bloods Range Formation|69153|5|Briefly described|500k_geologyp08_lut.csv||Mesoproterozoic|||Tjauwata Group|||Metamorphosed sandstone and siltstone, and felsic and mafic schist derived from volcanic rock|
36765|Bloods Range Formation|69436|5|Briefly described|p21:4, 13-14, 19|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Clastic red bed succession. Deformed in the Wankari Detachment Zone of the Petermann Nappe Complex, with growth of kyanite, phlogopite and muscovite.||Tjauwata Group.||Transitionally overlies Puntitjata Rhyolite and Wankari Volcanics.|Conglomerate, fine sandstone and siltstone, grading upwards into immature sandstone. North of Wankari Detachment Zone, comprises gritty and pebbly quartz-muscovite schist, muscovite quartzite, and kyanite-muscovite-phlogopite-quartz schist.|12-JUL-16
36765|Bloods Range Formation|69438|5|Briefly described|p23:9|Mesoproterozoic|Mesoproterozoic|Alluvial-fluvial deposits.||Tjauwata Group.||Is overlain disconformably by Kulail Sandstone.||12-JUL-16
36765|Bloods Range Formation|70018|4|Described|p233,235-236|Mesoproterozoic|Mesoproterozoic|Amadeus Basin. Interbedded siliciclastic sedimentary rocks.||Unit of Tjauwata Group.||Uppermost unit of Tjauwata Group. Underlain by Wankari Volcanics.|Red shale, polymictic conglomerate, volcaniclastics, tuffaceous layers and local lensoidal quart sandstone beds.|
36765|Bloods Range Formation|70634|4|Described|500k_geolgyp08_lut.csv|Mesoproterozoic|Mesoproterozoic|||Tjauwata Group|||Metamorphosed sandstone and siltstone, and felsic and mafic schist derived from volcanic rock.|
36765|Bloods Range Formation|70793|4|Described|500k_interpgeop14_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Events: Giles Event (1085-1040 Ma); Areyonga Movement; Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Alice Springs Orogeny (450-295 Ma).|1085-1040 Ma (inferred)|Unit of Tjauwata Group.|||Metamorphosed basalt, basaltic tuff, conglomerate, and quartzite|
36765|Bloods Range Formation|70839|5|Briefly described|p345|||Mineralogically immature, including arkose and conglomerates; similar clasts assemblage to Mount Currie Conglomerate and Mutitjulu Arkose.||Unit of Tjauwata Group.||||
36765|Bloods Range Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone, schist, shale|
36765|Bloods Range Formation|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|1030-1030 Ma (inferred)|Unit of Tjauwata Group.|||Metamorphosed sandstone and siltstone, and felsic and mafic schist derived from volcanic rock|
36765|Bloods Range Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Tjauwata Group|||Metamorphosed sandstone and siltstone, and felsic and mafic schist derived from volcanic rock.|
32054|Blue Billy Formation|22897|6|Mentioned|102|||Geol province Bangemall Basin. Parent Edmund Group.||||||08-SEP-08
32054|Blue Billy Formation|22905|5|Briefly described|p52 Fig. 2, p53 Table 1|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group.  Max. thickness: 500 m. Overlain by Cheyne Springs Formation Overlies the Gooragoora Formation.||||||24-JAN-06
32054|Blue Billy Formation|23403|4|Described|p7|Mesoproterozoic|Mesoproterozoic|Of Edmund Group.||||||
32054|Blue Billy Formation|23780|5|Briefly described|p17|Proterozoic|Proterozoic|Of the Edmund Group.||||||
32054|Blue Billy Formation|24115|4|Described|p4 Fig.2|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group. Maximum Thickness: 500m. Overlies the Gooragoora Formation. Overlain by the Cheyne Springs Formation. Geological Province: Edmund Basin.||||||
32054|Blue Billy Formation|24183|2|Defined|p1, p11|Stenian||Newly defined unit (Martin, D. McB. & Thorne, A. M. 2002). Max. Thickness: 500m. Overlies the Gooragoora Formation. Overlain by the Cheyne Springs Formation. Age: >1072 +/- 8 Ma.||||||08-SEP-08
32054|Blue Billy Formation|24544|4|Described|p44 Fig.32|Mesoproterozoic|Mesoproterozoic|Of Edmund Group. Overlies Gooragoora Formation. Overlain by Cheyne Springs Formation.||||||
32054|Blue Billy Formation|50225|4|Described|p387 Fig. 2, p393|||Of Edmund Gp. Together with Muntharra Fm replaces part of former Jillawarra Fm. Conformably overlies Gooragoora Fm; downlaps onto Irregully Fm. Transitional with conformably overlying Cheyne Springs Fm.  Max. thick: 500m.||||||07-FEB-11
32054|Blue Billy Formation|50226|6|Mentioned|p428|||Supersedes Jillawarra Formation of Cooper et al (1998). Of the Edmund Group.||||||08-SEP-08
32054|Blue Billy Formation|50292|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Geological Province: Edmund Basin. Of the Edmund Group (Bangemall Supergroup). Overlies: Gooragoora Formation. Underlies: Cheyne Springs Formation, Kiangi Creek Formation.||||||07-NOV-08
32054|Blue Billy Formation|50312|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Edmund Group. Geological Province: Edmund Basin. Siltstone and mudstone; minor thin- to thick-bedded sandstone; locally sulfidic.||||||31-MAY-04
32054|Blue Billy Formation|50313|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup).  Geological Province: Edmund Basin. Underlies: Cheyne Springs Formation. Overlies: Gooragoora Formation.||||||07-NOV-08
32054|Blue Billy Formation|50380|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin.||||||07-NOV-08
32054|Blue Billy Formation|60301|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin. Siltstone and mudstone, sandstone.||||||07-NOV-08
32054|Blue Billy Formation|63470|5|Briefly described|Map legend||Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin. Siltstone and mudstone; minor thin- to thick bedded sandstone; locally sulfidic.||||||07-NOV-08
32054|Blue Billy Formation|63471|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin. Siltstone and mudstone; minor thin- to thick-bedded sandstone; locally sulfidic.||||||07-NOV-08
32054|Blue Billy Formation|63866|5|Briefly described|p162|||||Edmund Group||||
32054|Blue Billy Formation|63869|4|Described|p28-29, p30, p31-32, p43, Plate 1|Calymmian|Statherian|Of Martin and Thorne (2002). Partly equivalent to the Jillawarra Formation of Muhling and Brakel (1985). Thickness generally <200 m, but ranges from 0-500 m. An important exploration target for sediment-hosted Cu, Pb, Zn.|c.1620-1465 Ma.|Unit in Edmund Group.||Overlies Gooragoora Formation conformably and Irregully Formation disconformably. Is overlain disconformably by Kiangi Creek Formation, and gradationally by Cheyne Springs Formation.|Distinctive parallel-planar laminated, black, pyritic, carbonaceous, fissile to flaggy siltstone that weathers to a blue-grey colour; local bodies of thick-bedded, massive coarse-grained quartz sandstone, dolomitic sandstone, and pebbly sandstone.|
32054|Blue Billy Formation|64287|5|Briefly described|p31, p34 Fig. 2|||Sandstone, siltstone unit on EDMUND sheet.||||||07-FEB-11
32054|Blue Billy Formation|64580|4|Described|map legend||Mesoproterozoic|Of Edmund Group. Siltstone and mudstone; sandstone, and dolostone; locally sulfidic.||||||
32054|Blue Billy Formation|64728|5|Briefly described|pp95-96, pp99-100, pp103-104.|Mesoproterozoic|Mesoproterozoic|Deeper marine siliciclastic and carbonate facies.|Contains detrital zircons clustered  c.1790 Ma.|Unit in Edmund Group.||Overlies Gooragoora Formation. Is overlain by Cheyne Springs Formation.|Planar-laminated, carbonaceous siltstone; lesser lithic quartz sandstone, silicified siltstone.|
32054|Blue Billy Formation|65830|4|Described|p4-6, p9-10, p13, p15, Plates 1-2|Calymmian|Statherian|Formerly Jillawarra Formation. Up to 500m thick. Transgressive deposit of deep marine anoxic mudstone; turbidite and mass flow deposits. Hosts the Reiffel Zinc prospect . Intruded by a 1070 Ma dolerite sill.||Of the Edmund Group||?Unconformably underlain by Gooragoora Formation. Underlain by Irregully Formation. Overlain gradationally by Cheyne Springs Formation. Disconformably overlain by Kiangi Creek Formation.|Parallel-planar-laminated, black, pyritic, carbonaceous, fissile to flaggy siltstone. Contains massive, medium to coarse-grained quartz sandstone bodies interbedded with planar laminated siltstone and minor dolostone.|
32054|Blue Billy Formation|66241|6|Mentioned|pp1-4. |||||Unit in Edmund Group.||Overlies Gooragoora Formation. Is overlain by Cheyne Springs Formation.||
32054|Blue Billy Formation|67136|5|Briefly described|Map legend.|||Edmund Basin.||Unit in Edmund Group.||Overlies Irregully Formation. Is overlain by Kiangi Creek Formation.|Siltstone and mudstone; minor thin- to thick-bedded sandstone; locally sulfidic.|
32054|Blue Billy Formation|67374|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Edmund Basin.||Unit in Edmund Group.|||Siltstone and mudstone; minor thin- to thick-bedded sandstone; locally sulfidic.|
32054|Blue Billy Formation|68285|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin.||Of the Edmund Group.||Underlain by the Irregully Formation. Overlain by the Kiangi Creek Formation or Cheyne Springs Formation.|Siltstone and mudstone; minor thin- to thick-bedded sandstone; locally sulfidic.|
32054|Blue Billy Formation|68286|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin.||Of the Edmund Group||Underlain by the Irregully Formation. Overlain by the Cheyne Springs Formation.|Siltstone and mudstone; minor thin- to thick-bedded sandstone; locally sulfidic.|
32054|Blue Billy Formation|69003|5|Briefly described|p34|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||Edmund Group.||Overlies Gooragoora Formation. Is overlain by Cheyne Springs Formation.||
32054|Blue Billy Formation|69024|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin. Includes an unnamed subunit mapped separately, of medium- to thick-bedded sandstone and siltstone, locally sulfidic.||Of the Edmund Group.||Conformably underlain by the Gooragoora Formation and overlain by the Cheyne Springs Formation.|Siltstone and mudstone; minor thin- to thick-bedded sandstone; locally sulfidic.|05-MAY-14
32054|Blue Billy Formation|69027|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Of the Edmund Group.||Underlain by the Gooragoora Formation. Overlain by the Cheyne Springs Formation.|Siltstone and mudstone; minor thin- to thick-bedded sandstone; locally sulfidic.|05-MAY-14
32054|Blue Billy Formation|69028|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin. Mapped with Gooragoora and Cheyne Springs Formations as one unit.||Of the Edmund Group.|||Siltstone and mudstone, sandstone and dolostone; locally sulfidic.|06-MAY-14
32054|Blue Billy Formation|69166|4|Described|geologyp_lut.csv|Mesoproterozoic|Paleoproterozoic|Age derived from lithic quartz sandstone (148971.1.pdf)|1746 Ma +/- 8 Ma (SHRIMP)|Edmund Group||Unconformably overlies Irregully Formation, Conformably overlies Gooragoora Formation, Conformably overlain by Cheyne Springs Formation|Mudstone; minor thin- to thick-bedded sandstone and siltstone; locally sulfidic|
32054|Blue Billy Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|||Part of Edmund Group, Depositiional package 2.||Unit of Edmund Group.||||
32054|Blue Billy Formation|69596|6|Mentioned|p12 Fig.7, p17|||Edmund Basin.||Edmund Group.||||
32054|Blue Billy Formation|70019|5|Briefly described|p93-94|Mesoproterozoic|Mesoproterozoic|Geological province: Gascoyne Province, Capricorn Orogen.||Unit of Edmund Group.||Overlain by Cheyne Springs Formation. Underlain by Gooragoora Formation.||
32054|Blue Billy Formation|70767|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Edmund Basin. Section only: no outcrop in map area.||Edmund Group.||Overlies Irregully Formation. Is overlain by Kiangi Creek Formation.|Siltstone and mudstone; minor thin- to thick-bedded sandstone; locally sulfidic.|
32054|Blue Billy Formation|70768|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Edmund Basin. Section only: no outcrop in map area.||Edmund Group.||Overlies Irregully Formation. Is overlain by Kiangi Creek Formation.|Siltstone and mudstone; minor thin- to thick-bedded sandstone; locally sulfidic.|
32054|Blue Billy Formation|70795|4|Described|100k_geologyp_lut.csv|Mesoproterozoic|Paleoproterozoic|Also 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 148971.1.pdf, West Australian Craton, Edmund Basin|1679-1517 Ma|Edmund Group||Unconformably overlies Irregully Formation, Conformably overlies Gooragoora Formation, conformably overlain by Cheyne Springs Formation, overlain disconformably by Kiangi Creek Formation|Lithic quartz sandstone, carbonaceous siltstone and mudstone, medium to thick bedded sandstone and siltstone; locally sulfidic.|
32054|Blue Billy Formation|70814|4|Described|p3, p5, p8-p10, p20, p22, p24-p25|||Edmund Basin. Together with the Gooragoora and Cheyne Springs Formations forms Depositional Package 2 of the Edmund Group. Up to 800m thick but is generally less than 200m thick. Interpreted as a basinwide deposit of mostly deep-marine anoxic mud alongside turbidite mass-flow deposits. Age poorly constrained. Intruded by the Kulkatharra and Narimbunna Dolerites.||Edmund Group||Conformably overlies the Gooragoora Formation. Disconformably overlies the Irregully Formation. Conformably overlain by the Cheyne Springs Formation.|Black, pyritic, carbonaceous, fissile to flaggy siltstone interbedded with subordinate sandstone, dolomitic siltstone and chert.|
32054|Blue Billy Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, mudstone, sandstone|
32054|Blue Billy Formation|72705|5|Briefly described|p3-4|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen. Deep-water shelf deposits.||Edmund Group.||Overlies Gooragoora Formation. Is overlain by Cheyne Springs Formation.|Pyritic carbonaceous siltstone and turbidite.|
32054|Blue Billy Formation|73442|6|Mentioned|p23|||Also referred to as Depositional Package 2.||||Intruded by Kulkatharra Dolerite||
75662|Bobbie Point Metasyenogranite|67380|5|Briefly described|p9-10, p22|Statherian|Statherian|Eastern Biranup Zone, Albany-Fraser Orogen. Oldest intrusive rock in the Biranup Zone. Its Hf signature is compatible with its main source being reworked Archean Yilgarn Craton margin. Appears as Bobbie Point metasyenogranite on p9.|1708 +/- 15 Ma.|||||
75662|Bobbie Point Metasyenogranite|68186|5|Briefly described|p19, p39, p78-79, Plates 1A, 2|Paleoproterozoic|Paleoproterozoic|Forms rocky ridges. Emplaced during early stages of Biranup Orogeny.|1708 +/- 15 Ma (Kirkland et al., 2010).||||Pink, medium- to coarse-grained, seriate to equigranular, variably strained and mylonitized metasyenogranite; weak to moderate, NE-trending foliation. Includes minor mingled mafic rocks and minor BIF rafts.|
75662|Bobbie Point Metasyenogranite|69743|6|Mentioned|p191|Paleoproterozoic|Paleoproterozoic|Biranup Zone.|c.1708 Ma.|||||
75662|Bobbie Point Metasyenogranite|70089|6|Mentioned|p263|Paleoproterozoic|Paleoproterozoic|Tropicana Zone, NE Albany-Fraser Orogen.||||||
75662|Bobbie Point Metasyenogranite|70182|5|Briefly described|p4-5, p25, p30, p46|Paleoproterozoic|Paleoproterozoic|Tropicana Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen. Formed during Biranup Orogeny. Archean crustal source. Anomalous composition (described) compared with immediately older and younger granite groups.|c.1710 Ma.||||A-type granite.|
75662|Bobbie Point Metasyenogranite|70256|5|Briefly described|p4-5|Paleoproterozoic|Paleoproterozoic|Kirkland et al. (2010). Tropicana Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen.|c.1708 Ma.|||||
75662|Bobbie Point Metasyenogranite|70802|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Geological province: Kepa Kurl Booya Province, Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage I (1330-1260 Ma); Albany-Fraser Orogeny Stage II (1225-1140 Ma); Biranup Orogeny (1710-1620 Ma). Sample GSWA 194737 (metasyenogranite) yielded a weighted mean 207Pb*/206Pb* date of 1708+\-15 Ma, interpreted as magmatic crystallisation age of the syenogranite. See 500k_interpgeop14_lut.csv, 250k_pre_mesozoic_interpgeop_lut.csv.|1708+\-15 Ma||||Metasyenogranite; weakly foliated to mylonitic; includes minor mingled mafic rocks and minor banded iron-formation rafts; may include remnants of McKay Creek Metasyenogranite|
75662|Bobbie Point Metasyenogranite|70826|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|Intruded during intracratonic reactivation of the Capricorn Orogen.||||||
75662|Bobbie Point Metasyenogranite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Tropicana Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen.|1708+/-15 Ma.|||May intrude McKay Creek Metasyenogranite. May include remnants of McKay Creek Metasyenogranite, and Tropicana or Hercules Gneiss.|Metasyenogranite; weakly foliated to mylonitic; includes minor mingled mafic rocks and rafts of banded iron-formation; may include remnants of McKay Creek Metasyenogranite, and Tropicana or Hercules Gneiss.|
75576|Boee beds|65074|4|Described|p351, p353, p357 Tb. 4-12, p358|Neoproterozoic|Neoproterozoic|Of NW Birrindudu Basin. Reference area is east of Baines Hills. 350 m thick.||||Probably equivalent to Erica Sandstone. Probably unconformably overlies Jawilga beds.|Medium- to fine-grained sublithic arenite with interbedded conglomerate.|
75576|Boee beds|69440|5|Briefly described|p25:1, 3|Cryogenian|Cryogenian|Crops out as narrow strike ridges E of the Baines Hills in BILLILUNA map area. Resembles Erica Sandstone. The conglomerate beds occur in the unit's reference area in the SW part of the outcrop area.||||Conformably overlies Jawilga beds. Correlates with Erica Sandstone.|Mainly sublithic arenite; local conglomerate beds.|12-JUL-16
75576|Boee beds|71080|6|Mentioned|p4|||Of Blake et al. 1977, 1979. Previously considered potential correlative of Erica Sandstone.||||||
75576|Boee beds|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Medium to fine grained lithic sandstone with minor conglomerate|
23402|Bolgumirri Member|13194|4|Described|p395 Tb. 4-16, p399 fig 4-63|||Type Section: 2km E of Clark Jump Up 15o26'S 128o39'E. Up to 44m subtidal ooid shoal deposits.||Skewthorpe Formation||Overlies Djigumirri Member (conformably).|Oolitic dolomite and sandy dolomite.|
23402|Bolgumirri Member|40993|6|Mentioned|Fig.1|||||||||
23402|Bolgumirri Member|41864|4|Described|p39|||||||||
23405|Bongabinni Formation|14228|5|Briefly described|p6 fig3|Caradoc|Caradoc|South Canning Basin.||Carribuddy Group||Overlies Nita Formation. Overlain by Minjoo Salt.||05-OCT-16
23405|Bongabinni Formation|22753|5|Briefly described|Fig.3 p585|Ordovician|Ordovician|||||||
23405|Bongabinni Formation|24449|5|Briefly described|p739|Llandeilian|Llanvirnian|Of Carribuddy Group.  Geological Province: Canning Basin.  See also p473 Fig. 5.||||||
23405|Bongabinni Formation|40837|2|Defined|p257 Fig. 4, p258, 274|Pridolian|Late Ordovician|Basal unit of the newly revised Carribuddy Group. Replaces Unit E of Carribuddy Formation. See also Fig. 5 page insert (p258).||||||17-FEB-10
23405|Bongabinni Formation|42030|6|Mentioned|p746|||||||||
23405|Bongabinni Formation|43563|6|Mentioned|Fig.2,p5|||||||||
23405|Bongabinni Formation|43599|6|Mentioned|p250, Fig.3|Caradocian|Llanvirnian|||||||
23405|Bongabinni Formation|43656|6|Mentioned|Fig.2,p8|Caradocian|Llanvirnian|||||||
23405|Bongabinni Formation|43666|6|Mentioned|p49,Table 2||Ordovician|||||||
23405|Bongabinni Formation|43746|6|Mentioned|Fig.2,p11|Caradocian|Llanvirnian|||||||
23405|Bongabinni Formation|43818|6|Mentioned|Fig.2.p39||Silurian|||||||
23405|Bongabinni Formation|44143|4|Described|p.440 Table 4-19; p.442, Figure 4-96|Silurian|Silurian|Unit in Carribuddy Group. Up to 208m thick; red-brown claystone & dolomite; sabkha and supratidal marine. Conformably overlain by Mount Troy Formation. Type section between 4071 & 4279m in Kidson 1 (URAL: 22deg 37' 27" S, 125 deg 00' 17" E). Contains rare spores & pollen.||||||22-NOV-17
23405|Bongabinni Formation|61021|5|Briefly described|p36 Fig. 2|Llanvirnian|Llanvirnian|Of the Carribuddy Group. Contains shaly source rocks for hydrocarbons and algal coals. Geological Province: Canning Basin.||||||17-DEC-07
23405|Bongabinni Formation|61551|5|Briefly described|p351 Fig.2, p355, p359.|Late Ordovician|Darriwilian|Onshore Canning Basin. Has excellent hydrocarbon source and seal potential.||Unit in Carribuddy Group.||Overlies Goldwyer Formation.|Shales.|
23405|Bongabinni Formation|64334|5|Briefly described|p39, 43|Ordovician|Ordovician|Canning Basin; subsurface only. Caradoc. Contains beds of algal oil shale with TOC up to 62 percent along the Admiral Bay Fault Zone.||Carribuddy Group.||Overlies Nita Formation. Is overlain by Minjoo Salt and Mount Troy Formation.|Mudstone.|
23405|Bongabinni Formation|64643|5|Briefly described|p3 Fig. 2|Upper Ordovician|Middle Ordovician|Of Carribuddy Group?||||||
23405|Bongabinni Formation|64982|5|Briefly described|p698.|Early Ordovician|Early Ordovician|Thickness to 200 m; supratidal to continental environment. Acts as seal for Nita Formation hydrocarbon reservoir.||Basal unit in Carribuddy Group.||Is overlain by Minjoo Salt and Mount Troy Formation.|Red-brown claystones and minor dolomite.|
23405|Bongabinni Formation|65301|5|Briefly described|p5 Fig. 4, p8 Fig. 5|Late Ordovician|Middle Ordovician|Geological province: Canning Basin.||||||
23405|Bongabinni Formation|65449|4|Described|p1, p6-9, p13-14, p17-19, p21, p23|Late Ordovician|Middle Ordovician|See also p34-38, p40, p47-50, p53-58; Plates 1-10. Lehmann (1984), after Bongabinni Native Well. Type section is the interval 4279-4071m in Kidson 1. Contains excellent oil-prone source rocks along the Admiral Bay Fault Zone; variously referred to as algal coal or oil shale (geochemical and petrological properties detailed). Biostratigraphic data detailed.||Carribuddy Group.||Overlies Nita Formation conformably and gradationally in most areas. Is overlain by Minjoo Salt.|Dominantly red-brown mudstone, often calcareous or dolomitic, with interbeds of argillaceous dolomite and rare thin beds, veins and scattered crystals of halite and anhydrite.|
23405|Bongabinni Formation|67888|6|Mentioned|p82|||||||||
23405|Bongabinni Formation|68007|4|Described|p1-2, p4, p11-12, p14-15, Plates 1, 2|Late Ordovician|Middle Ordovician|Canning Basin. About 130m thick. Oil and gas shows. Excellent local source potential; poor reservoir potential. Composite well log.||Basal Carribuddy Group.||Overlies Goldwyer Formation. Is overlain by Minjoo Salt.|Dominated by greenish-grey to light grey (red brown near the top) claystone and siltstone, often calcareous; interbeds of very fine- to fine-grained, well sorted sandstone in the upper part. Interbeds of limestone throughout.|24-FEB-20
23405|Bongabinni Formation|68902|5|Briefly described|p9 fig 5|Ordovician|Ordovician |||Carribuddy Group||Overlies Nita Formation, overlain by Nibil Formation.||
23405|Bongabinni Formation|69029|5|Briefly described|p316,319-320,333|Darriwilian|Darriwilian|Of Canning Basin. Thickness: 208m in Kidson-1, <100m thick in Willaea Sub-basin and Broome Platform, 30m on terrace areas (Haines, 2004). Contains the richest source rocks in the Canning Basin. Mainly developed in the southern Canning. Organic-rich shales are oil-prone with TOC up to 60%.||||Overlain by Minjoo Salt. Underlain by Goldwyer Formation.|Red-brown mudstone.|
23405|Bongabinni Formation|69182|6|Mentioned|Ch4 p9-p12, Ch4 p40-p41|Upper Ordovician|Upper Ordovician|Canning Basin. See also Ch4 p45, Ch4 p47, Ch4 p50-p58, Ch4 p74, Ch4 p79-p82.||Carribuddy Group||Overlies the Nita Formation. Overlain by the Minjoo Salt and the Nibil Formation.||
23405|Bongabinni Formation|69297|6|Mentioned|p350, p354|Silurian|Late Ordovician|Canning Basin. Contains good potential oil source rocks. ||Carribuddy Group||||
23405|Bongabinni Formation|69312|5|Briefly described|p1, p3, p7, p9, p13 fig 13-14|Middle Ordovician|Middle Ordovician|Canning Basin. Contains oil-prone source rocks. In places contains a TOC of up to 60 percent. See also  p14 fig 15-16, p15, p19, p24 fig 28, p25 fig 30, p27 fig 34, p28 fig 36, p29, p30, p31. ||Carribuddy Group||Overlies the Nita and Goldwyer Formations. Overlain by the Minjoo Salt and the Mount Troy Formation.|Red-brown mudstone and shale.|
23405|Bongabinni Formation|69883|5|Briefly described|p4-p6, p12-p13, p24, p27|Caradoc|Llanvirn|Canning Basin. Supersequences provided. Contains potential petroleum source rocks. See also p34, p38, plate 1-2, plate 4.||Carribuddy Group||Conformably (gradational) overlies the Nita Formation. Overlain by the Minjoo Salt and Mount Troy Formation.|Redbed evaporitic mudstone and minor carbonate and sandstone.|
23405|Bongabinni Formation|70061|6|Mentioned|Regional geology p8|||Canning Basin. Oil-prone.||||||12-JUL-16
23405|Bongabinni Formation|70065|6|Mentioned|Regional: p5-6|Ordovician|Ordovician|Willara Sub-basin. These sub-salt organic-rich shales locally have excellent source quality.||||||
23405|Bongabinni Formation|70774|5|Briefly described|p4|Late Ordovician|Middle Ordovician|Willara and Kidson Sub-basins, Canning Basin.||Carribuddy Group||Overlies the Nita Formation. Overlain by the Minjoo Salt and Nibil Formation.||06-FEB-20
23405|Bongabinni Formation|71171|6|Mentioned|p2|||Canning Basin.||||||
23405|Bongabinni Formation|71870|5|Briefly described|p1, p3|Ordovician|Ordovician|Canning Basin. A petroleum source interval formed during the Larapintine petroleum supersystem.||Carribuddy Group||Overlies the Nita Formation. Overlain by the Minjoo Salt.||
23405|Bongabinni Formation|71894|5|Briefly described|p4|Upper Ordovician|Upper Ordovician|Canning Basin.||Carribuddy Group||Overlies the Nita Formation. Overlain by the Minjoo Salt.|Shale.|
23405|Bongabinni Formation|72497|5|Briefly described|p3 Fig.2.|Middle Ordovician|Middle Ordovician|Shown as occuring in the Anketell, Tabletop, Ryan Shelves, Willara and Kidson Sub-basins, the Jurgurra and Barbwire Terraces and Broome Platform. Age given as Llanvirnian~= Darriwilian.||Carribuddy Group||Conformably overlies Goldwyer and Nita Formations and underlies Minjoo Salt and Mt Troy Formation.||
23405|Bongabinni Formation|72499|5|Briefly described|p7 Fig.6.|Late Ordovician|Late Ordovician|Located in the Broome Platform.||Carribuddy Group||Overlies Nita Formation and underlies Minjoo Salt, Nibil Formation.|Includes shale.|
23405|Bongabinni Formation|73117|5|Briefly described|p3, p32|Upper Ordovician|Upper Ordovician|Hydrocarbon source interval.||Carribuddy Group||Underlain by Nita Formation. Overlain by Minjoo Salt.|Dominantly shale and mudstone.|
23405|Bongabinni Formation|73344|6|Mentioned|p6|Sandbian|Darriwilian|Canning Basin, subsurface. Part of supersequence B1.||Carribuddy Group||Underlain by Nita Formation. Overlain by Minjoo Salt / Mount Troy Formation.||
23405|Bongabinni Formation|73346|6|Mentioned|p27|||Canning Basin. Basal unit of the Carribuddy Group. Includes a fine-grained sandstone unit in the upper portion.||Carribuddy Group||||
39732|Bonney Downs Monzogranite|24193|5|Briefly described|p875 Fig.2|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
39732|Bonney Downs Monzogranite|63441|5|Briefly described|p12 tb. 2|Archean|Archean|Of Split Rock Supersuite. Supersedes Bonney Downs Granite. Age: 2838+/-6Ma. Geological province: Pilbara Craton.||||||07-FEB-11
39732|Bonney Downs Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|Age derived from biotite monzogranite sample (178014.1.pdf)|2861 +/- 4 Ma (SHRIMP)|Split Rock Supersuite|||Monzogranite; medium grained; locally sparsely porphyritic; locally muscovite-bearing. Pegmatite and leucocratic, medium grained, muscovite monzogranite with abundant xenoliths of granitic gneiss.|
39732|Bonney Downs Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; Split Rock Supersuite Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|2838 Ma (isotopic; inferred)|Unit of Split Rock Supersuite.|||Pegmatite and leucocratic, medium-grained, muscovite-bearing monzogranite; also variably porphyritic, with xenoliths of greenstone and granitic gneiss.|
39732|Bonney Downs Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
39732|Bonney Downs Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||2838+/-6 Ma|Split Rock Supersuite|||Monzogranite; medium grained; locally sparsely porphyritic; locally muscovite bearing.|
39732|Bonney Downs Monzogranite|72668|6|Mentioned|p11|||Intrudes the Kurrana Terrane.|c. 2840Ma|||||
32179|Bonnie Vale Tonalite|43232|5|Briefly described|Map Legend||Archean|||||||11-JUN-15
32179|Bonnie Vale Tonalite|65204|5|Briefly described|p18, p19 Tbl.4,|Neoarchean||2680+/-5 Ma (U-Pb zircon; Hill et al. 1992); 1-5mm grains; equigranular.||||||11-JUN-15
32179|Bonnie Vale Tonalite|69152|4|Described|1m_geologyp08_lut.csv|Archean|Archean||||||Tonalite; mafic granite.|05-AUG-15
32179|Bonnie Vale Tonalite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2680 +/- 5 Ma (isotopic).||||Biotite-bearing tonalite; medium- to coarse-grained, equigranular; massive; intruded by auriferous laminated quartz reefs; metamorphosed.|
32179|Bonnie Vale Tonalite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||tonalite|
32179|Bonnie Vale Tonalite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 1m_geologyp12_lut.csv.|2680+\-5 Ma||||Biotite-bearing tonalite; medium- to coarse-grained, equigranular; massive; intruded by auriferous laminated quartz reefs; metamorphosed|
34483|Bonsers Claystone|22769|5|Briefly described|Table1p759||Holocene|||||||
79197|Booanya Suite|70182|5|Briefly described|p8-9, p33-34, p38, p41, p45-47|Mesoproterozoic|Mesoproterozoic|New name, after Booanya Rock, NE of Esperance. Stage II of the Albany-Fraser Orogeny. Restricted to eastern Nornalup Zone. Trace-element enriched granites. Geochemistry detailed; magmatic evolution discussed. Strongly magnetic.||Esperance Supersuite.|||Granites, ferroan, alkali-calcic to alkalic; characteristically strongly enriched in REE. A-type.|
79197|Booanya Suite|70802|5|Briefly described|250k_pre_mesozoic_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage II (1225-1140 Ma); Albany-Fraser Orogeny (1330-1140 Ma).|1198-1140 Ma (inferred)|Unit of Esperance Supersuite.|||Undeformed to weakly deformed granites; typically porphyritic|
79197|Booanya Suite|71270|4|Described|500k_interpgeop16_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage II (1225 - 1140 Ma); Albany-Fraser Orogeny (1330 - 1140 Ma).|1198-1140 Ma (inferred)|Unit of Esperance Supersuite.|||Undeformed to weakly deformed granites; typically porphyritic|
79197|Booanya Suite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Albany-Fraser Orogen.||Esperance Supersuite|||Undeformed to weakly deformed granites; typically porphyritic.|
79197|Booanya Suite|72710|5|Briefly described|p10.|Stenian|Stenian|Part of the Albany-Fraser Orogen.|1198 Ma to 1140 Ma.|Esperance Supersuite|||Includes megacrystic monzogranite and syenogranite.|
79197|Booanya Suite|73084|5|Briefly described|p: 24,56,63-64,79,83,96,98,~124-127,134.|Stenian|Stenian|Madura Province. Albany-Fraser Orogen. Includes monzonite from the Hannah prospect [informally referred to as Hannah monzonite not as a unit name]. Became increasingly juvenile with decreasing age. Part of a regionally extensive, high-temperature event named the Maralinga Event by Spaggiari et al. (2016). Report includes whole-rock geochemistry, Sm-Nd.|1182-1170 Ma [?]|Esperance Supersuite||||
34997|Boodalla Suite|23046|5|Briefly described|169|||||||||
74954|Boodanoo Suite|64891|5|Briefly described|p37 Fig. 2, p42, p50-51 Tb. 1|Archean|Archean|Of Annean Supersuite. Contains the Narndee Igneous Complex. Age: c.2780Ma. Geological province: Murchison Domain. Layered gabbro, with dunite, pyroxenite, anorthosite, and hornblende gabbro; includes younger leucogabbro; metamorphosed||||||07-FEB-11
74954|Boodanoo Suite|66195|5|Briefly described|p604, p605, p598 Fig.1, p599 Fig.2|Neoarchean|Mesoarchean|Yilgarn Craton. The Narndee Igneous Complex contains a large volume of hornblende gabbro, distinguishing it from the Meeline Suite. Age constraint from Sm-Nd isochron of 2824 +/-80 Ma from mineral seperates of Narndee Igneous Complex (Scowen 1991).|New SHRIMP date: 2800 +/- 6 Ma.||The main component identified to date is the Narndee Igneous Complex.|||13-MAR-12
74954|Boodanoo Suite|67129|5|Briefly described|p18 Fig.19, p19 Fig.20, p20, p51-54, p57|Archean|Archean|See also p60. Hosts some chromium, nickel, copper and PGE mineralization.|2800 +/- 6 Ma|Annean Supersuite|Narndee Igneous Complex||Mafic-ultramafic rocks.|06-SEP-17
74954|Boodanoo Suite|68107|6|Mentioned|p618||||c.2800 Ma (Van Kranendonk and Ivanic, 2009).||||Mafic and ultramafic layered intrusions.|
74954|Boodanoo Suite|68108|4|Described|p650, p651 Tb.4|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane.|2800 +/- 6 Ma; U-Pb (Ivanic et al. 2010).||||Differentiated igneous complexes.|
74954|Boodanoo Suite|68110|5|Briefly described|p673|Neoarchean|Mesoarchean|Murchison Domain. Appears as Boodanoo Mafic-Ultramafic Suite on p673, p674 Fig.2.|c.2815 - 2000 Ma.||Includes Narndee Igneous Complex.|||08-OCT-14
74954|Boodanoo Suite|68561|5|Briefly described|GEOCHRON files|||Murchison Domain, Youanmi Terrane. See geochron file 191056.1.pdf.||Annean Supersuite.|Includes Narndee Igneous Complex|Intrudes the Norie Group.||
74954|Boodanoo Suite|68698|5|Briefly described|p4-5, p9, p18|Mesoarchean|Mesoarchean|Large, layered mafic-ultramafic igneous complex. Contains V and minor Cu-Ni-PGE mineralisation.|c.2.81 Ga.|Annean Supersuite.||||
74954|Boodanoo Suite|69583|4|Described|p47, p49-50, p56, p98, p101-102, p177|||See also Plate 2. Northern Murchison Domain. Consists of the one unit. Igneous stratigraphic column.|c.2800 Ma.|Annean Supersuite.|Narndee Igneous Complex.||Layered gabbro, metamorphosed.|
74954|Boodanoo Suite|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean||||Narndee Igneous Complex|||
74954|Boodanoo Suite|69586|5|Briefly described|p22|Neoarchean|Mesoarchean|Murchison Domain.|||Narndee Igneous Complex.|||
74954|Boodanoo Suite|69626|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton||Annean Supersuite|Narndee Igneous Complex|||
74954|Boodanoo Suite|70020|5|Briefly described|p113,118,120,128|Neoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton. Comprises felsic rocks hosting VHMS mineralisation.|||Includes Narndee gabbro and Murroulli dolerite.||Komatiite and komatiitic basalt.|
74954|Boodanoo Suite|70030|5|Briefly described|p190|||Geological province: Murchison Domain, Yilgarn Craton. Mafic intrusive associated with Norie Group (Ivanic et al., 2010).||||||
74954|Boodanoo Suite|70419|5|Briefly described|p2, p8|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Mafic-ultramafic intrusives.|c.2.8 Ga.||Narndee Igneous Complex.|||
74954|Boodanoo Suite|70770|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c.2800 Ma.||Narndee Igneous Complex|||
74954|Boodanoo Suite|70796|4|Described|2_5m_interpgeop15_lut.csv|Neoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. Affected by the Yilgarn Craton granite magmatism (3010  2600 Ma); Youanmi Terrane events (3131  2600 Ma). See also 100k_geologyl_lut.csv, 100k_geologyp_lut.csv, 100k_geologysub_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeol_lut.csv,  500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 185995.1.pdf, 185996.1.pdf, 191056.1.pdf, 198210.1.pdf, Bungar100_2539_stratig.pdf. See also the entry for the Narndee Igneous Complex for additional lithologies. Numerous additional lithologies are discussed.|ca 2800 Ma|Annean Supersuite||Intrudes the Norie Group. Intruded by the Mount Kenneth Suite.|Layered maficultramafic intrusive rocks containing hornblende oikocrysts; extensively amphibolitized adjacent to shear zones; locally strongly sheared|
74954|Boodanoo Suite|70826|6|Mentioned|p8|Mesoarchean|Mesoarchean|Coincides with the deposition of the Norie Group.||||||
74954|Boodanoo Suite|70830|5|Briefly described|p2-p5, p9, p50, p57|Neoarchean|Neoarchean|Murchison Domain. This unit has an estimated length of 50km and estimated volume 2350 km^3.|2800 +/- 6 Ma (Ivanic et al., 2010)|Annean Supersuite|Includes the Narndee Igneous Complex.|||
74954|Boodanoo Suite|71168|5|Briefly described|p7, p19 fig 11|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. See also p22, p51, p59-61.|c. 2800 Ma||Includes the Narndee Igneous Complex, Narndee gabbro and the Murrouli dolerite.||Granitic rocks.|
74954|Boodanoo Suite|71269|4|Described|2_5m_interpgeop15_lut.csv|Neoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Of Narndee Igneous Complex. Scowen (1991) reported Sm-Nd whole-rock isochron date of 2824+\-80 Ma for the Narndee Igneous Complex. Sample GSWA 191056 (gabbronorite) yielded a weighted mean 207Pb/206Pb date of 2799+\-7 Ma, interpreted as the igneous crystallization age of the gabbronorite. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See also geochron files.|2800 Ma (inferred)|Unit of Annean Supersuite.||Intruded by Mount Kenneth Suite. Intrudes into Norie Group/Murchison Group.|Layered mafic-ultramafic intrusive rocks containing hornblende oikocrysts; extensively amphibolitized adjacent to shear zones; locally strongly sheared.|
74954|Boodanoo Suite|71272|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Annean Supersuite.|Fields Find Igneous Complex.|||
74954|Boodanoo Suite|71809|5|Briefly described|map legend|Archean|Archean|Yilgarn Craton||Of Annean Supersuite.|Includes Fields Find Igneous Complex.|||06-SEP-19
74954|Boodanoo Suite|72034|6|Mentioned|500k_interpgeop16_lut|Neoarchean|Mesoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Narndee Igneous Complex.|||
81966|Boogardie Orbicular Granite|72724|4|Described|p24-26|Neoarchean|Neoarchean|Small shallow, saucer-shaped intrusion (sill) within a porphyritic monzogranite pluton of regional extent. Outcrop on Boogardie Station called 'Pretty Rock' since the 1880s. Highly prized as an ornamental dimension stone, and is displayed as highly polished slabs and blocks in the geological collections of museums worldwide. U-Pb SHRIMP analyses done on the very small (100-200 microns) zircons. Two samples provided indistinguishable results, and 39 zircon analyses were combined to yield an average date of 2691.5+/- 1.9 Ma, interpreted as the crystallisation age.|2691.5 +/- 1.9 Ma U-Pb SHRIMP crystallisation age.|||Hosted by a regionally extensive porphyritic monzogranite pluton, crystallisation age range 2706 - 2700 Ma. Cut by pegmatite veins, crystallisation age 2691.5 +/- 1.1 Ma from titanite by ID-TIMS.|Subspherical orbicules, about 5 to 15 cm diameter, within a medium to coarse-grained granitic matrix. The distinctive orbicules are composed of concentric shells of radiating hornblende and plagioclase feldspar crystals.|29-JUN-20
68501|Bookargemoona Tonalite|63441|2|Defined|p46 Appx.1, p7 Tb. 2|Archean|Archean|Of Tambina Supersuite. Age: 3427 +/- 4 Ma, 3435 +/- 3 Ma. Intruded by Carbana Monzogranite. Geol.prov: East Pilbara Terrane. Strongly foliated to gneissic biotite tonalite, containing greenstone xenoliths; the gneissic compositional layering is complexly folded||||||15-APR-13
68501|Bookargemoona Tonalite|64621|5|Briefly described|Map legend|Archean|Archean|Of the Tambina Supersuite. Meta-biotite tonalite; folaited to gneissic; local xenoliths of amphibolite.||||||07-NOV-08
68501|Bookargemoona Tonalite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Tambina Supersuite. Age shown as 3427-3408 Ma. Meta biotite tonalite; foliated to gneissic; local xenoliths of amphibolite.||||||
68501|Bookargemoona Tonalite|69012|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane.|c. 3427 Ma|Of the Tambina Supersuite.|||Comprises meta biotite tonalite; foliated to gneissic; local xenoliths of amphibolite.|
68501|Bookargemoona Tonalite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Tambina Supersuite|||Meta biotite tonalite; foliated to gneissic; local xenoliths of amphibolite|
68501|Bookargemoona Tonalite|69566|6|Mentioned|p236|||Corunna Downs Granitoid Complex, East Pilbara Granite-Greenstone Terrane.||||||
68501|Bookargemoona Tonalite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|3427 Ma (isotopic)|Unit of Tambina Supersuite.|||Metamorphosed biotite tonalite; foliated to gneissic; local xenoliths of amphibolite|
68501|Bookargemoona Tonalite|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||tonalite, granodiorite|
68501|Bookargemoona Tonalite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||3427+/-4 Ma.|Tambina Supersuite|||Metamorphosed biotite tonalite; foliated to gneissic; local xenoliths of amphibolite.|
29942|Bookingarra Group|23783|5|Briefly described|p3|||||||||
29942|Bookingarra Group|23784|5|Briefly described|p20|Archean|Archean|Age: 2965-2942Ma.||||||07-NOV-08
29942|Bookingarra Group|23789|4|Described|p21|Archean|Archean|Age: 2975-2950Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
29942|Bookingarra Group|23793|4|Described|p7|Archean|Archean|Age: c. 2975-2950Ma||||||07-NOV-08
29942|Bookingarra Group|23813|5|Briefly described|p90 Tb. 1|Archean|Archean|Conglomerate, epiclastic sediments, slate, tholeiitic and high-Mg basalts, amygdaloidal basalts.  Age: 2.965-2.95Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.||||||07-NOV-08
29942|Bookingarra Group|24023|5|Briefly described|p6|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
29942|Bookingarra Group|24140|3|Fully described|p216, p214 Fig. 1|Archean|Archean|Redefined to include Negri Volcanics.  Comprises Cistern Formation, Rushall Slate and Negri Volcanics. Volcaniclastic sandstone, chert and shale. Overlies Whim Creek Group. Min.age: 2975+/-4Ma. Geological province: Mallina Basin. See also p217.||||||07-NOV-08
29942|Bookingarra Group|24184|4|Described|p714, p715 Fig.11|Archean|Archean|Geological Province: Mallina Basin. Age: ca.2948-2942Ma (Pb isotope)||||||07-NOV-08
29942|Bookingarra Group|24185|5|Briefly described|p739 Tb.3|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
29942|Bookingarra Group|24191|4|Described|p829, p828 Fig.1|Archean|Archean|New unit which includes rocks previously included in Whim Creek Group; suggestion that this unit forms part of Mallina Basin.  Age: 2975+/-4Ma; min. age: 2955-2945Ma (Smithies et al, 2001).  Overlies Whim Creek Group.  Geological Province: Pilbara Craton.||||||07-NOV-08
29942|Bookingarra Group|24192|5|Briefly described|p860|Archean|Archean|Overlying Unit: Whim Creek Group. Geological Province: Pilbara Craton. Includes the Rushall Slate and Cistern Formation. Age: ca. 2975 Ma||||||07-NOV-08
29942|Bookingarra Group|24541|6|Mentioned|p19 Fig. 5|||Of the Pilbara Supergroup.||||||
29942|Bookingarra Group|24550|5|Briefly described|p36 Tb. 3.2|Archean|Archean|Clastic sediments, basalt, rhyolite. Age: 2975Ma. In the Whim Creek Belt. Geological Province: Pilbara Craton. See also p74 Tb. 5.1.||||||07-FEB-11
29942|Bookingarra Group|50302|5|Briefly described|Map Legend|Archean|Archean|Of the Pilbara Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
29942|Bookingarra Group|50430|5|Briefly described|p158 Tb.1||Archean|In Mallina Basin.||||||07-NOV-08
29942|Bookingarra Group|60362|4|Described|p1516, p1518|Archean|Archean|NW Mallina Basin. Sediments sourced from Whim Creek Group filled local fault-bound depocentres.|||Louden, Mount Negri Volcanics.|Unconformably overlies Whim Creek Group.|Fine- to coarse-grained sediments. Volcaniclastic turbidites dominate the lower part; siliciclastic turbidites dominate up-sequence.|
29942|Bookingarra Group|61253|5|Briefly described|p56|Archean|Archean|Basal unit of De Grey Supergroup. Overlain by Croydon Group. Age: ~3.02-2.97Ga. Geological Province: western Pilbara Craton/ Mallina Basin. See also p50 Fig. 1, p52 Fig. 2.||||||07-NOV-08
29942|Bookingarra Group|63372|5|Briefly described|Map Legend|Archean|Archean|Of the Pilbara Supergroup. Geological Province: Whim Creek and Mallina Basin||||||07-NOV-08
29942|Bookingarra Group|63441|5|Briefly described|p5 tb. 1, p14 Fig. 2|Archean|Archean|Redefined as Bookingarra Formation.||||||07-FEB-11
29942|Bookingarra Group|69299|4|Described|p6 Tb.1, p7, p8 Fig.5, p9 Tb.2, p21|Archean|Archean|Mallina Basin. Concealed on COOYA POOYA. Unconformably overlies Whim Creek Group constituents and is regionally overlain unconformably by Mount Roe Basalt (Fortescue  Group) on COOYA POOYA.|||Includes Kialrah Rhyolite, Mount Negri Volcanics, Louden Volcanics, Rushall Slate, Cistern Formation.||Dominantly basaltic.|
29942|Bookingarra Group|69300|5|Briefly described|map legend|Archean|Archean|Mallina Basin, Whim Creek greenstone belt.||Pilbara Supergroup|Kialrah Rhyolite, Mount Negri Volcanics, Louden Volcanics, Rushall Slate, Cistern Formation|||08-SEP-15
29942|Bookingarra Group|70775|2|Defined|iii, p10, p12-p13, p94-p95|Mesoarchean|Mesoarchean|Mallina Basin. Name derived from Bookingarra Creek. The name was first used to formally name a succession of five formations that unconformably overlies the Whim Creek Group. Van Kranendonk et al. (2006) included those formations in the Croydon Group based on an interpretation of stratigraphic continuity between the successions of the Whim Creek greenstone belt and the adjacent Mallina Basin. This interpretation is no longer accepted as structural and geochronological data indicate that the units correlated have different ages and are located on opposite sides of a regional unconformity. See also the Bookingarra Formation which is an obsolete term used by Van Kranendonk et al (2006) to refer only to the succession of the Louden Volcanics and Mount Negri Volcanics. Distribution, mineralization, age and depositional environment are discussed. This Group has a maximum thickness of 3000m in the eastern half of the Whim Creek greenstone belt. The type area is Bookingarra Creek to Mount Negri, 5km northeast of Whim Creek mine.  Metamorphosed volcaniclastic conglomerate, sandstone, siltstone, shale and minor chert are present also. See also p38-p39, p41, p44 fig 27, p45, p51, p55-p56, p60, p62, p64, p65, p72, p75, p81, .|c. 2955-2948 Ma|De Grey Supergroup|Includes the Cistern Formation, Rushall Slate, Louden Volcanics, Kialrah Rhyolite, Mount Negri Volcanics and the Opaline Well Intrusion.|Unconformably overlies the Whim Creek Group. Unconformably overlain by the Fortescue Group. Faulted against the Croydon Group.|Komatiite, komatiitic basalt, tholeiitic basalt, andesite, dacite and rhyolite. Subvolcanic sills of peridotite, pyroxenite, gabbro and dolerite are common and local stocks of dacite and rhyolite also occur.|
29942|Bookingarra Group|72251|5|Briefly described|p54|Mesoarchean|Mesoarchean|Geological province: West Pilbara Superterrane, Pilbara Craton.||Unit of De Grey Supergroup.|Includes Rushall Slate, Cistern Formation and Mallina Formation.|||
29942|Bookingarra Group|72668|6|Mentioned|p14, p17|||Downgraded and incorporated into Croyden Group.||||||
23409|Boondawari Formation|22589|6|Mentioned|p125||Proterozoic|||||||
23409|Boondawari Formation|22716|6|Mentioned|table4, p230|Neoproterozoic III|Neoproterozoic III|Age: 610 Ma||||||
23409|Boondawari Formation|22816|5|Briefly described|p8 Table 1|||Savory Group||||||
23409|Boondawari Formation|22901|4|Described|74|||Geol province Officer Basin. Max thickness 800 m||||||
23409|Boondawari Formation|22907|3|Fully described|40|||||||||
23409|Boondawari Formation|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Officer Basin.||||||
23409|Boondawari Formation|23557|5|Briefly described|p95 Fig.1|Neoproterozoic III|Neoproterozoic III|Geological Province: Officer Basin.||||||
23409|Boondawari Formation|23590|5|Briefly described|p5 fig. 2|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
23409|Boondawari Formation|23602|4|Described|p17|Cryogenian|Cryogenian|Age: 670 Ma. Of Savory Group. Underlain by Mundadjini Formation.||||||23-MAR-06
23409|Boondawari Formation|23730|4|Described|p12|Neoproterozoic|Neoproterozoic|Overlying unit Disappointment Group. Underlying unit Mundadjini Formation. Geological Province: Officer Basin.||||||
23409|Boondawari Formation|23758|5|Briefly described|p2 Fig 1|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
23409|Boondawari Formation|23760|4|Described|p30|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
23409|Boondawari Formation|24390|5|Briefly described|p11 Fig. 6|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
23409|Boondawari Formation|24594|5|Briefly described|p602 Fig. 1|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin (Paterson Orogen).||||||
23409|Boondawari Formation|41768|2|Defined|Table 5|Precambrian||||||||
23409|Boondawari Formation|42708|5|Briefly described|Plate 1|Proterozoic||||||||
23409|Boondawari Formation|43229|5|Briefly described|Map Legend||Neoproterozoic|Of Savory Group.||||||11-APR-08
23409|Boondawari Formation|43492|3|Fully described|9|||||||||
23409|Boondawari Formation|43756|4|Described|Fig.1,p534,537-39|||||||||
23409|Boondawari Formation|43848|5|Briefly described|Map Legend||Proterozoic|||||||
23409|Boondawari Formation|44111|6|Mentioned|p.58 Fig. 2, p59|||in Savory Basin. Unit in Savory Group. Includes tillites, correlated with Marinoan glaciation; equivalent to Supersequence 3 of Centralian Superbasin.||||||
23409|Boondawari Formation|50008|5|Briefly described|p45 Fig.2|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin||||||
23409|Boondawari Formation|50085|5|Briefly described|p11 Fig. 6|Neoproterozoic|Neoproterozoic|Age: ~600Ma.  Geological Province: Officer Basin.||||||
23409|Boondawari Formation|50188|5|Briefly described|p10 Fig. 3, p17|||Geological Province: Officer Basin. Intruded by "Boondawarri Dolerite".||||||16-JUL-08
23409|Boondawari Formation|60470|6|Mentioned|p3, Fig. 1|Neoproterozoic|Neoproterozoic|in Officer Basin||||||
23409|Boondawari Formation|61023|5|Briefly described|p15 Fig. 8|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||11-APR-08
23409|Boondawari Formation|61716|6|Mentioned|p641, p650|||||||||10-MAY-06
23409|Boondawari Formation|61732|3|Fully described|p4 Fig. 3, p87-88|Ediacaran|Ediacaran|Disconformably or unconformably overlain by, or faulted against, Diasappointment Gp units - McFadden and Tchukardine Fms; disconformable or unconformable on Mundadjini Fm. Thick: up to 800m. See also p56, p58 Fig. 22, p5 Tb. 1.||||||07-FEB-11
23409|Boondawari Formation|62453|3|Fully described|p5 Fig. 3, 12 Fig. 8, 22, 58|Ediacaran|Cryogenian|Geological Province: Officer Basin. Overlies: Sunbeam Group, Mundadjini Formation. Underlies: McFadden Formation. Diamictite, sandstone, siltstone, conglomerate, mudstone, dolomite. Thickness: ~800m. ||||||
23409|Boondawari Formation|62987|6|Mentioned|p30|||Geological Province: northwestern Officer Basin.||||||25-JAN-07
23409|Boondawari Formation|63022|5|Briefly described|p1014|||Part of the Marinoan glacial succession. Supersequence 3. ||||||
23409|Boondawari Formation|64103|6|Mentioned|p400, p400 Fig. 3|Ediacaran|Ediacaran|Geological Province: Officer Basin. Glacial.||||||07-FEB-11
23409|Boondawari Formation|64580|4|Described|map legend||Neoproterozoic|Conglomerate; sandstone; siltstone; diamictite, dolomite; fluvial, coastal and fluvioglacial origin.||||||09-DEC-08
23409|Boondawari Formation|64722|6|Mentioned|Fig. 6 p15|Neoproterozoic|Neoproterozoic|Of Officer Basin, Centralian Superbasin.||||||
23409|Boondawari Formation|64725|6|Mentioned|p67.|Neoproterozoic|Neoproterozoic|Officer Basin.||||||
23409|Boondawari Formation|64772|5|Briefly described|p13, p15, Plate 1, p14 Fig.7, p20-21|Neoproterozoic|Neoproterozoic|Overlies Sunbeam Group. Unconformably overlain by McFadden Fm (Diasappointment Gp). Age: c.600Ma. Geological province: Officer Basin.|||||Glacigenic diamictite, sandstone, siltstone, and shale; diamictite commonly overlain by red-brown, coarse- to medium-grained flaggy sandstone, which is  interbedded with sandy siltstone and cobble conglomerate lenses|25-NOV-13
23409|Boondawari Formation|64777|5|Briefly described|p2 Fig.3 |Neoproterozoic|Neoproterozoic|||||||
23409|Boondawari Formation|64970|6|Mentioned|p719 Fig. 2|Ediacaran|Marinoan|Geological Province: Officer Basin.||||||27-MAY-09
23409|Boondawari Formation|65363|6|Mentioned|p5 Fig.4, p8, p18.|Neoproterozoic|Neoproterozoic|Northwestern Officer Basin. Correlated with Wahlgu Formation.||||||
23409|Boondawari Formation|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Cryogenian|Northwestern Officer Basin||||||
23409|Boondawari Formation|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Cryogenian|Northwestern Officer Basin||||||
23409|Boondawari Formation|65403|5|Briefly described|p29.|||Glacigenic deposits.|>610 Ma.|Unit in Savory Group.||||
23409|Boondawari Formation|65410|5|Briefly described|p74.|||Savory Sub-basin. Compares lithologically and in isotope chemostratigraphy with Supersequence 3 units elsewhere in the Centralian Superbasin; Julie Formation (Amadeus Basin) and the upper Wonoka Formation (Adelaide Geosyncline).|||||Tillite, siltstone and carbonate.|
23409|Boondawari Formation|65416|5|Briefly described|p137, p141, p146.|Marinoan|Marinoan|Officer Basin. Part of Supersequence LP3. Tentatively correlated with Pertatataka Formation (Amadeus Basin).|||||Diamictite, conglomerate, sandstone, siltstone, shale and carbonates, including distinctive oolitic and pisolitic limestone and stromatolitic dolomite.|
23409|Boondawari Formation|65454|4|Described|p6, p7 Fig.3, p11, p30 Fig.A1b|Cambrian|Cryogenian|Of Officer Basin. Glacigene diamictite, sandstone, siltstone, conglomerate and shale. Similarities to Supersequences 3 and 4 of Centralian Superbasin. Overlies Mundadjini Formation and overlain unconformably by Tchukardine Formation. >508 +/- 5 Ma intrusive dolerite dykes.||||||21-APR-16
23409|Boondawari Formation|65826|5|Briefly described|p3 Fig.1, p15.|Neoproterozoic|Neoproterozoic|Officer Basin. Glacigene rocks.|c.610 Ma.|||||
23409|Boondawari Formation|67195|5|Briefly described|p10 fig 6|Neoproterozoic|Neoproterozoic|Western Officer Basin.|||||Sandstone.|
23409|Boondawari Formation|67202|5|Briefly described|p60, p64|||Officer Basin.|c.610 Ma.||||Diamictite, sandstone and shale.|
23409|Boondawari Formation|68270|4|Described|p678,680-684,687|Ediacaran|Cryogenian|Western Officer Basin. Type section is in Boondawari Creek east of Boondawari Soak; lat., 23'31'32"S, long., 121'29'57"E. Poorly exposed unit in the NW Officer Basin; less than 800m thick. Glacio-marine deposit. Lower section contains diamictite and is a correlative to Elatina Formation, and Wanapi Dolomite Member. Upper section is lithologically similar to Pertatataka Formation. The lower Boondawari is laterally equivalent to the Wahlgu Formation.||||Underlain disconformably by Sunbeam Group, Mundadjini Formation; unconformably by basement. Overlain unconformably by McFadden Formation.|Diamictite (dark grey to purple mudstone containing pebble-boulder clasts), lenticular interbeds of sandstone and very pooly sorted conglomerate, siltstone, mudstone, dolomitic siltstone, dolomite.|03-JUL-19
23409|Boondawari Formation|68277|6|Mentioned|p96|Neoproterozoic|Neoproterozoic|The rank is not given in the text.||||||
23409|Boondawari Formation|68902|5|Briefly described|p5-6, p20, p25|Ediacaran|Ediacaran|7km thick. Intruded by granitic bodies. Diamictites were largely derived from the Paterson Orogen. Intruded by c.508 Ma mafic dyke swarms.||||Is overlain unconformably by the Disappointment Group.|Includes diamictites.|
23409|Boondawari Formation|69003|6|Mentioned|p4, p60|Ediacaran|Ediacaran|NW Officer Basin. Paterson Orogen.||||||
23409|Boondawari Formation|69185|5|Briefly described|500k_geologyp08_lut.csv||Neoproterozoic||||||Undivided; conglomerate; sandstone; siltstone; diamictite, dolomite; fluvial, coastal and fluvioglacial origin|
23409|Boondawari Formation|71169|5|Briefly described|p16|Ediacaran|Cryogenian|Officer Basin.|635-580 Ma (inferred age)|||||
23409|Boondawari Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone, conglomerate, diamictite|
23409|Boondawari Formation|72034|5|Briefly described|500k_interpgeop16_lut|Ediacaran|Cryogenian|Officer Basin (Phase 1).|||||Diamictite, conglomerate, sandstone, siltstone, dolomite; fluvial, coastal and fluvioglacial origin.|
77196|Bootenall Limestone Member|61811|5|Briefly described|p32.|Pleistocene|Pleistocene|||Unit in Tamala Limestone.||Disconformably overlies Cape Burney Sandstone Member.|Reef limestone; massive accumulation of collapsed coral fronds of Acropora.|
25804|Borda Sandstone|22718|5|Briefly described|P9, Table1 P6||Tertiary|||||||
25804|Borda Sandstone|23722|6|Mentioned|p36|Tertiary|Tertiary|Geological Province: Canning Basin||||||
25804|Borda Sandstone|30897|5|Briefly described|p19|||||||||
25804|Borda Sandstone|32648|6|Mentioned|p32|||Tertiary||||||
25804|Borda Sandstone|36257|6|Mentioned|Table 2.1|||||||||
25804|Borda Sandstone|36890|4|Described|p355|||||||||
25804|Borda Sandstone|38886|6|Mentioned|Map legend|Tertiary|Tertiary|Prob. Tertiary||||||
25804|Borda Sandstone|42814|5|Briefly described|p24|||||||||
25804|Borda Sandstone|44998|2|Defined|p195-6||Cenozoic|Overlies Pender Bay Conglomerate. Cainozoic.||||||19-NOV-08
25804|Borda Sandstone|45153|2|Defined|App.11-167|late Tertiary|late Tertiary|||||||
25804|Borda Sandstone|61155|5|Briefly described|p16|Middle Eocene|Middle Eocene|Age: ~50.5-~44.5Ma. Thickness: 5m. Geological Province: Dampier Peninsula.||||||
25804|Borda Sandstone|64449|6|Mentioned|p62 Tb. 2|Tertiary|Tertiary|Consists of fine sand.||||||07-FEB-11
38672|Border Group|23787|5|Briefly described|p69 Fig. 35|Archean|Archean|Geological Province: Windimurra Complex.||||||07-NOV-08
38672|Border Group|70419|5|Briefly described|p7|||Ahmat (1986). The border zone of the Complex, between sheared supracrustal rocks and the lower zone gabbros. Typically 100m thick.||Windimurra Igneous Complex.|||Dolerite; typically recrystallised at amphibolite facies. Includes Norie Group wall rocks / xenoliths.|
38656|Bore Well Complex|23786|5|Briefly described|p24|||Not a stratigraphic name.  Geological Province: Yilgarn Craton.||||||
38656|Bore Well Complex|24494|6|Mentioned|p19|||||||||
38656|Bore Well Complex|63980|4|Described|pp59-61.|Archean|Archean|NNW-striking volcanic-volcaniclastic succession, probably representing thrust-fault repetitions of a single large volcanic centre. Dominantly andesitic; minor dacites, rhyolites and intrusions. Age is for a rhyolitic volcaniclastic rock within the Complex.|2708 +/- 4 Ma.||||Volcaniclastic sandstones and poorly-sorted, quartz-poor, matrix-supported breccias, oligomictic to polymictic; fine-grained sedimentary rocks: silicified quartz-poor siltstones, interbedded with sandstone, and more-massive fine-grained breccias.|25-SEP-14
38656|Bore Well Complex|65264|5|Briefly described|p19|||Located on LAKE CAREY map sheet. Andesite and plagioclase(-hornblende) porphyritic andesite are dominant rock types.||||||07-FEB-11
38656|Bore Well Complex|66880|6|Mentioned|p16, p27. |Archean|Archean||2708 +/- 4 Ma.|||||24-SEP-14
38656|Bore Well Complex|68109|5|Briefly described|p660|Neoarchean|Neoarchean|Locally layered with thin units of komatiite.|ca. 2720-2700 Ma||||Mafic volcanic rocks and calc-alkaline complexes.|
25805|Boronia Swamp Alluvium|37341|2|Defined|p246|Eocene|Late Cretaceous|Late Cretaceous or Eocene||||||
28391|Bossut Formation|7433|5|Briefly described|pp50-51.|Cainozoic|Cainozoic|Canning Basin.  Some outcrops in western Dampier Peninsula form arcuate semi-submerged reefs up to 1 km offshore.|||||Coastal limestones; cross-bedded eolian carbonate-cemented sandstones; unlithified beach ridge deposits.|
28391|Bossut Formation|22717|5|Briefly described|P14||Quaternary|Equivalent to the Tamala Limestone.||||||01-OCT-08
28391|Bossut Formation|22718|5|Briefly described|P9, Table1 P6||Quaternary|||||||
28391|Bossut Formation|22738|4|Described|9,14,15,17, map|Quaternary|Quaternary|Max thickness 10 m. Underlying unit Parda Formation||||||
28391|Bossut Formation|22765|5|Briefly described|P11, Table1||Quaternary|||||||
28391|Bossut Formation|23484|6|Mentioned|p36|||||||||
28391|Bossut Formation|23793|6|Mentioned|p42|||||||||
28391|Bossut Formation|32648|6|Mentioned|p32|||Pleistocene||||||
28391|Bossut Formation|35711|5|Briefly described|p28|||See also Table 3,stratigraphy. Hydrogeology on P36.||||||
28391|Bossut Formation|35969|6|Mentioned|Table 6|||||||||
28391|Bossut Formation|36890|4|Described|p356|||||||||
28391|Bossut Formation|37368|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
28391|Bossut Formation|37370|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
28391|Bossut Formation|37564|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
28391|Bossut Formation|37577|6|Mentioned|p75|||||||||
28391|Bossut Formation|38886|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
28391|Bossut Formation|39697|6|Mentioned|p140|||||||||
28391|Bossut Formation|40045|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
28391|Bossut Formation|40078|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
28391|Bossut Formation|41271|6|Mentioned|p197|||||||||
28391|Bossut Formation|42571|5|Briefly described|Table1 P8|||||||||
28391|Bossut Formation|43307|5|Briefly described|Map Legend||Pleistocene|||||||
28391|Bossut Formation|43563|6|Mentioned|Fig2,p5|Pleistocene|Pliocene|||||||
28391|Bossut Formation|43818|6|Mentioned|Fig.2.p39||Cenozoic|||||||19-NOV-08
28391|Bossut Formation|44143|4|Described|p.429 Table 4-19|Cainozoic|Cainozoic|Max. thickness 33m; calcarenite, calcirudite, with varying amounts of quartz grains, and lenses of calcilutite; partly oolitic; coastal dunes and beach. Type area: coast near Wallal Station. Disconformably overlies Broome Sandstone and Parda Formation. Varied fauna of foraminifera and molluscs.||||||
28391|Bossut Formation|44536|14|Not recorded|map legend||Pleistocene|||||||
28391|Bossut Formation|44998|2|Defined|p199|||Shore-line deposit. Overlies Frezier Sandstone & Parda Formation. =?Coastal Limestone?||||||
28391|Bossut Formation|45153|2|Defined|App.11-166|Quaternary|late Tertiary|Late Tertiary to Quaternary. See also Table 1, P4.||||||
28391|Bossut Formation|45158|6|Mentioned|p11|||||||||
28391|Bossut Formation|61155|5|Briefly described|p16||Pleistocene|Thickness: 10m. Geological Province: Southern Canning Basin and Dampier Peninsula.||||||
28391|Bossut Formation|64449|4|Described|p63-64|Quaternary|Quaternary|Calcarenites. Detailed disscussion on correct definition of this unit.||||||07-FEB-11
28391|Bossut Formation|68283|5|Briefly described|Map Legend|Quaternary|Quaternary||||||Calcarenite; minor calcirudite and calcilutite.|07-JAN-15
28391|Bossut Formation|69590|4|Described|100k_geologyp_lut.csv|Pleistocene|Pleistocene|Of Canning Basin.|1.8-0.01 Ma (inferred)||||Calcarenite; minor calcirudite and calcilutite|
79173|Bottle Corner Shoshonite|71143|5|Briefly described|p431-433|Stenian|Stenian|Geological province: Coompana Province. Bimodal magmatism. Typically formed from post-orogenic extensional melting of subduction-modified lithosphere as a resulting of upwelling asthenosphere. Mafic shoshonites forms a minor component of the Loongana core in the Madura Province, intruding into c. 1400 Ma rocks. Here, geochemistry indicate possible derivation from thinner crust, and a source with less subduction-modification.|1192-1180 Ma|Unit of Moodini Supersuite.||||
79173|Bottle Corner Shoshonite|71165|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Moodini Supersuite.|||Diorite to metamonzodiorite.|
79173|Bottle Corner Shoshonite|72947|6|Mentioned|p14|Stenian|Stenian|Coompana Province, western.|c. 1192-1180 Ma|||May correlate to Merdayerrah Shoshonite.||30-NOV-22
79173|Bottle Corner Shoshonite|73084|4|Described|p: 15, 39, 43-45, 69, 73, ~101-110...|Stenian|Ectasia|Coompana Province, and[?] Madura Province. Isotopically primitive. Became increasingly juvenile with decreasing age. Dates are magmatic crystalisation ages from the FOR010 drillcore. Also records a number of inherited grain ages. Report includes lithologic/petrographic description, structural analysis, whole-rock geochemistry, geochronology, Sm-Nd. Also p: 124, 128-129, 134-136.|1175 +/- 5 Ma, 1184 +/- 8 Ma, 1192 +/- 13 Ma|Moodini Supersuite|||Metamorphosed and evolved Si-rich shoshonite including hornblende metadiorite to metamonzodiorite, and unfoliated porphyritic and equigranular syenogranite veins.|
79173|Bottle Corner Shoshonite|73224|5|Briefly described|p42, p44|Stenian|Stenian|Product of mantle input and the assimilation of crust similar to the Bunburra and Koomalboogurra suites. Represents melting of subduction-enriched lithosphere during extension and mantle upwelling.|c. 1174 Ma||||Mafic-intermediate composition.|
79173|Bottle Corner Shoshonite|73225|5|Briefly described|p18|||Western Coompana Province. Represents melting of subduction-enriched lithosphere during extension and mantle upwelling.||Moodini Supersuite.||||
69576|Bottle Creek Microgranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Feldspar- and quartz-phyric microgranite; metamorphosed.|05-AUG-15
69576|Bottle Creek Microgranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|See also 500k_interpgeop14_lut.csv.|2700 +/- 9 Ma (isotopic).||||Feldspar- and quartz-phyric microgranite; metamorphosed.|
69576|Bottle Creek Microgranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv.|2700+\-9 Ma ||||Feldspar- and quartz-phyric microgranite; metamorphosed|
69576|Bottle Creek Microgranite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||2700 +/-6 Ma.||||Feldspar- and quartz-phyric microgranite; metamorphosed.|
78349|Bounty Igneous Complex|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2698 - 2690 Ma (inferred).||||Dolerite, fine to medium grained, locally feldspar-phyric. Gabbro and pyroxenite, medium to coarse grained. Peridotite with cumulate texture and minor pyroxenite. All metamorphosed.|
78349|Bounty Igneous Complex|71212|4|Described|intro p2|Neoarchean|Neoarchean|Yilgarn Craton. Incorporates rocks belonging to the informal Golden Empress Gabbro, Wildcat Gabbro, Mikado Gabbro Breakaways and the Knobbly Gabbro. |2698 +/- 1 Ma to 2711 +/- 4 Ma|||Overlies the Knobbly Gabbro. Overlain by the Never Can Tell Basalt.||
78349|Bounty Igneous Complex|73151|6|Mentioned|p3, p10|||Yilgarn Craton. Kalgoorlie Terrane, Agnew Greenstone Belt. Shown as Bounty IC on p3.|||||Dolerite.|
78349|Bounty Igneous Complex|73596|5|Briefly described|p1152, 1157, 1165, 1167|Neoarchean|Neoarchean|Lawlers Domain, Agnew-Wiluna Greenstone Belt.|2698 +/- 1 Ma.|||Intrudes Hickies Bore Basalt. Sills intrude the boundary between Songvang Basalt and overlying Never Can Tell Basalt.|Includes granophyre.|
78619|Bow Hill Lamprophyre Suite|69003|6|Mentioned|p5|||Halls Creek Orogen.||||||
78619|Bow Hill Lamprophyre Suite|69099|4|Described|interpgeol_lut.csv|Cryogenian|Cryogenian|Lamboo Province|||||Olivine-phlogopite lamprophyre and garnet-phlogopite lamprophyre.|30-JUL-15
78619|Bow Hill Lamprophyre Suite|69165|4|Described|100K_interpgeol_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Olivine--phlogopite lamprophyre and garnet--phlogopite lamprophyre|
78619|Bow Hill Lamprophyre Suite|69597|6|Mentioned|p5 fig 2b|||||||||
78619|Bow Hill Lamprophyre Suite|69634|4|Described|100k_interpgeol_lut.csv|Cryogenian|Cryogenian|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone. |815 Ma (Isotopic)||||Olivine-phlogopite lamprophyre and garnet-phlogopite lamprophyre|
78619|Bow Hill Lamprophyre Suite|70154|4|Described|100k_interpgeol_lut.csv||||||||Olivine-phlogopite lamprophyre and garnet-phlogopite lamprophyre.|
78619|Bow Hill Lamprophyre Suite|70731|6|Mentioned|p268|Tonian|Tonian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.||||||
78619|Bow Hill Lamprophyre Suite|70826|6|Mentioned|p13, p14 tbl 5|Tonian|Tonian||815 Ma|||||20-MAY-20
78619|Bow Hill Lamprophyre Suite|71267|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Events: North Australian Craton events (2500-250 Ma); Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Kalkarindji Supersuite Magmatic Event (511-511 Ma); Yampi Orogeny (1000-800 Ma). See 100k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv. |815+\-20 Ma (isotopic)||||Olivine-phlogopite lamprophyre and garnet-phlogopite lamprophyre|
31019|Bradley Basalt|23484|4|Described|p10 table 3|Archean|Archean|Of Whundo Group.  Maximum thickness: 4000m.||||||07-NOV-08
31019|Bradley Basalt|23784|5|Briefly described|p10|Archean|Archean|Of Whundo Group.||||||07-NOV-08
31019|Bradley Basalt|23789|5|Briefly described|p9 Tb. 2|Archean|Archean|Of the Whundo Group.  Max. thickness: 74,000m.  Age: 3115+/-5Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
31019|Bradley Basalt|23793|4|Described|p16|Archean|Archean|Of Whundo Group. See also page 11 table 2.  Age: 3115+/-5Ma.||||||07-NOV-08
31019|Bradley Basalt|23794|5|Briefly described|Map Legend|Archean|Archean|Of Whundo Group. Underlain by  Woodbrook Fm. Overlain by Tozer Formation. Geological Province: Pilbara Craton.||||||07-NOV-08
31019|Bradley Basalt|24023|5|Briefly described|p7 fig. 4|Archean|Archean|Of Whundo Group. Maximum thickness: >4000m.||||||07-NOV-08
31019|Bradley Basalt|24184|4|Described|p712 Tb.4|Archean|Archean|Of the Whundo Group. Overlain by Woodbrook Formation. Underlain by Tozer Formation. Geological Province: Pilbara Craton. Max Thickness: >4000m. Age: 3115 +/- 5Ma||||||07-NOV-08
31019|Bradley Basalt|24353|4|Described|p9 Fig.5, p11 Tb.2|Archean|Archean|Of the Whundo Group. Age: 3115 +/- 5Ma. Max Thickness: >4000m. Geological Province: Pilbara Craton||||||07-NOV-08
31019|Bradley Basalt|24541|3|Fully described|p11 Tb.2, p22, p23|Archean|Archean|Of the Whundo Group. Age: 3115 +/-5 Ma. Maximum Thickness: >4000m. Conformably overlies the Tozer Formation. Conformably overlain by the Woodbrook Formation.||||||07-NOV-08
31019|Bradley Basalt|24543|5|Briefly described|Map legend|Archean|Archean|Of the Whundo Group (Pilbara Supergroup).  Age: c.3115Ma.  Pillow basalt, massive basalt, dolerite sills and minor felsic tuff and chert.||||||07-NOV-08
31019|Bradley Basalt|24550|5|Briefly described|p36 Tb. 3.2|Archean|Archean|Of the Whundo Group. Succession of massive and pillow basalts with high-Mg near base, and minor felsic tuffs at the top. Age: 3115Ma. Thickness: >400m. Geological Province: Pilbara Craton. See also p39, p78 Fig. 5.2.||||||07-FEB-11
31019|Bradley Basalt|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Age: <3.1Ga.  Geological Province: Pilbara Craton.||||||07-NOV-08
31019|Bradley Basalt|63372|4|Described|Map Legend|Archean|Archean|Of the Whundo Group. Geological Province: West Pilbara Granite-Greenstone Terrane. Age: 3115Ma. Pillow basalt, massive basalt, dolerite sills, and minor units of fel;sic pyroclastic rocks and chert; metamorphosed.||||||07-NOV-08
31019|Bradley Basalt|63441|4|Described|p5 Tb.1, p24|Archean|Archean|Of Whundo Group. Conformably overlies Tozer Formation; conformable below Woodbrook Fm. Thickness: 4000m. Geol. province: West Pilbara Superterrane. Comprises metamorphosed, massive + pillowed basalt, with spinifex-textured komatiitic basalt near base.||||||07-FEB-11
31019|Bradley Basalt|63538|4|Described|p6 Fig. 3|Archean|Archean|Of Whundo Group. Overlain by Woodbrook Formation, underlain Tozer Formation. Geological Province: Pilbara Craton.||||||19-APR-13
31019|Bradley Basalt|64174|5|Briefly described|Map legend|Archean|Archean|Of the Whundo Group. Age: c.3115Ma. Pillow basalt, massive basalt, dolerite sills, and minor felsic tuff, sandstone, shale and chert; metamorphosed.||||||07-NOV-08
31019|Bradley Basalt|64580|4|Described|map legend||Mesoarchean|Of Whundo Group. Pillow basalt, massive basalt, dolerite sills, and minor felsic tuff, sandstone, shale and chert; metamorphosed.||||||15-DEC-08
31019|Bradley Basalt|64632|6|Mentioned|p203 Fig.2|||||Of the Whundo Group.||Underlain by the Tozer Formation.||
31019|Bradley Basalt|67201|4|Described|p7 Fig.4, p12 Tb.1, p15-18, p46, p48|Archean|Archean|In northwestern Pilbara Craton, West Pilbara Superterrane, Sholl Terrane, Whundo Basin. Thickness: > 4.0 km.|c. 3120 Ma|Whundo Group||Conformably overlies Tozer Formation. Is conformably overlain by Woodbrook Formation.|Pillow basalt, masive basalt, dolerite sills, and minor felsic tuff, sandstone, shale, and chert; komatiitic basalt near base; metamorphosed.|
31019|Bradley Basalt|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological province: West Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 3115 Ma|Unit of Whundo Group.|||Pillow basalt, massive basalt, dolerite sills, and minor felsic tuff, sandstone, shale and chert; metamorphosed|
31019|Bradley Basalt|69299|5|Briefly described|p6 Tb.1|Mesoarchean|Mesoarchean|Concealed on COOYA POOYA. Thickness on COOYA POOYA: >4000 m.|3115 +/- 5 Ma||||Pillow basalt, massive basalt, and minor units of felsic tuff, tuffaceous sedimentary rocks, and chert.|
31019|Bradley Basalt|69300|5|Briefly described|map legend|Archean|Archean|West Pilbara Granite-Greenstone Terrane. Isotopic age: shown on legend as c. 3115 Ma|3115 +/- 5 Ma (isotopic age, Nelson 1996)|Whundo Group|||pillowed basalt, massive basalt, dolerite sills, and minor units of felsic tuff and chert; metamorphosed|02-SEP-14
31019|Bradley Basalt|69301|4|Described|p5 Fig.3, p9 Tb.1|||Pilbara Craton. West Pilbara Superterrane. Whundo Basin. Sholl Terrane. Thickness: >4.0 km.|3120 Ma|Whundo Group||Conformably overlies Tozer Formation. Is conformably overlain by Woodbrook Formation.|Mafic volcanic rocks. Consists of metamorphosed, massive and pillowed basalt, with komatiitic basalt near its base.|
31019|Bradley Basalt|70022|6|Mentioned|p115|||West Pilbara Superterrane.||Whundo Group.||||
31019|Bradley Basalt|70775|4|Described|p12, p15|Mesoarchean|Mesoarchean|Whundo Basin. This unit is more than 4000m thick. See also p25 tbl 4, p32, p33 fig 21, p35-p36, p41.|c. 3118-3115 Ma|Whundo Group||Conformably overlies the Tozer Formation. Overlain by the Woodbrook Formation.|Pillow basalt, massive basalt, dolerite sills and minor felsic tuff, sandstone, shale and chert; metamorphosed.|
31019|Bradley Basalt|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Whundo Basin.|max age 3118+/-3 Ma, min 3115+/-5 Ma.|Whundo Group|||Pillow basalt, massive basalt, dolerite sills, and minor felsic tuff, sandstone, shale and chert; metamorphosed.|
31019|Bradley Basalt|72251|5|Briefly described|p54|Mesoarchean|Mesoarchean|Geological province: West Pilbara Superterrane, Pilbara Craton.||||Overlain by Woodbrook Formation. Underlain by Tozer Formation.||
31019|Bradley Basalt|72668|6|Mentioned|p4, p13|||West Pilbara Superterrane.||Whundo Group||Overlies the Tozer Formation. Overlain by the Woodbrook Formation.||12-JAN-22
78404|Brady Well Monzogranite|65260|6|Mentioned|p6 Tb.1|Neoarchean||2658+/-13 Ma minimum age.||||||
74601|Brandy Well Monzogranite|60555|5|Briefly described|p4 Tb. 1|Archean|Archean|Age: 2658+/-13Ma (Swager & Nelson, 1997).||||||03-NOV-14
74601|Brandy Well Monzogranite|64340|6|Mentioned|p8 Tb. 1|||||||||
80121|Breakaways layered mafic-ultramafic complex|71212|4|Described|intro p2, intro p3, p58-59|||Yilgarn Craton. One of 5 informal units that are together equivalent to the formal Bounty Igneous Complex. Up to 800 metres thick. Parts of this complex are strongly magnetic. See also p46, p50, p53, p57, p89, p129, 257.||||Overlies the Knobbly Gabbro. Overlain by the Never Can Tell Basalt.|Massive, serpentinized dunite to peridotite, intensely foliated talc-tremolite-magnetite-carbonate schists.|26-SEP-17
38598|Breens Porphyry|23783|6|Mentioned|p55 Fig. 28|||||||||
27346|Bresnahan Group|22716|5|Briefly described|table4, p229|Paleoproterozoic|Paleoproterozoic|Deposited in the Bresnahan Basin.||||||07-NOV-08
27346|Bresnahan Group|23570|5|Briefly described|p14|||Geological Province: Pilbara Craton||||||
27346|Bresnahan Group|23575|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Overlain by Bangemall Group. Underlain by Mount Minnie Group.||||||18-JAN-07
27346|Bresnahan Group|23612|5|Briefly described|p839 Fig 2|Proterozoic|Proterozoic|||||||
27346|Bresnahan Group|24041|5|Briefly described|p492 Fig.1|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
27346|Bresnahan Group|24183|5|Briefly described|p2 Fig.1, p6|Paleoproterozoic|Paleoproterozoic|Geological Province: Ashburton Basin.||||||07-NOV-08
27346|Bresnahan Group|24544|4|Described|p43, p47 Fig.35|Paleoproterozoic|Paleoproterozoic|Unconformably overlies Wyloo Group's Capricorn Formation. Max. thickness: 4000 m. Conglomerate, sandstone and siltstone-mudstone. Geological Province: Ashburton Basin.||||||07-NOV-08
27346|Bresnahan Group|24607|6|Mentioned|p968 Fig. 1|||See also Bresnahan Formation.||||||30-NOV-10
27346|Bresnahan Group|29596|6|Mentioned|Table 1|||||||||
27346|Bresnahan Group|29916|6|Mentioned|p114|||||||||
27346|Bresnahan Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
27346|Bresnahan Group|30881|4|Described|p526|||||||||
27346|Bresnahan Group|30892|6|Mentioned|p100|||Middle Proterozoic||||||
27346|Bresnahan Group|31393|6|Mentioned|Pl.25|||||||||
27346|Bresnahan Group|31670|6|Mentioned|p911|||||||||
27346|Bresnahan Group|31828|6|Mentioned|p37|||Proterozoic. Map||||||
27346|Bresnahan Group|33540|6|Mentioned|Fig.2|||||||||
27346|Bresnahan Group|33544|5|Briefly described|p30|||Middle Prot.||||||
27346|Bresnahan Group|34115|6|Mentioned|p384|||Age: 1600-1700 my.||||||18-JAN-07
27346|Bresnahan Group|34135|4|Described|Table 2|||||||||
27346|Bresnahan Group|34287|6|Mentioned|p37|||||||||
27346|Bresnahan Group|34834|6|Mentioned|p219|||||||||
27346|Bresnahan Group|35260|6|Mentioned|p5|||Map legend||||||
27346|Bresnahan Group|35976|6|Mentioned|p107|||||||||
27346|Bresnahan Group|36003|6|Mentioned|Fig.8|||||||||
27346|Bresnahan Group|36883|3|Fully described|p143|||||||||
27346|Bresnahan Group|36891|4|Described|p442|||||||||
27346|Bresnahan Group|36902|6|Mentioned|p15|||||||||
27346|Bresnahan Group|37299|6|Mentioned|Fig.1|||||||||
27346|Bresnahan Group|37460|3|Fully described|p156|||||||||
27346|Bresnahan Group|37577|6|Mentioned|p6|||||||||
27346|Bresnahan Group|37707|6|Mentioned|Table I|||||||||
27346|Bresnahan Group|38298|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Lower Proterozoic||||||07-NOV-08
27346|Bresnahan Group|38299|5|Briefly described|p7|||||||||
27346|Bresnahan Group|38482|6|Mentioned|p15|||||||||
27346|Bresnahan Group|40089|6|Mentioned|p11|||||||||
27346|Bresnahan Group|40369|6|Mentioned|Fig.1|||||||||
27346|Bresnahan Group|40554|5|Briefly described|p29|||||||||
27346|Bresnahan Group|40904|6|Mentioned|p85|||||||||
27346|Bresnahan Group|40937|6|Mentioned|p5|||||||||
27346|Bresnahan Group|41125|6|Mentioned|p28|||||||||
27346|Bresnahan Group|41360|6|Mentioned|p192|||||||||
27346|Bresnahan Group|42013|5|Briefly described|Map Legend|Proterozoic||||||||
27346|Bresnahan Group|42148|6|Mentioned|Fig.3 P688|||||||||
27346|Bresnahan Group|42190|6|Mentioned|Fig.4 Map|||||||||
27346|Bresnahan Group|42260|4|Described|p99|||||||||
27346|Bresnahan Group|42435|6|Mentioned|p46|||||||||
27346|Bresnahan Group|42471|4|Described|p18|||In the Bresnahan Basin.||||||18-JAN-07
27346|Bresnahan Group|43561|5|Briefly described|Fig.3,1434,1436,1438|||||||||
27346|Bresnahan Group|44141|4|Described|p304-308|||First decribed by Talbot (1926); defined by Daniels and MacLeod (1965). The only lithostratigraphic unit in Bresnahan Basin. 4  km thick; capped by a BIF-derived conglomerate. Interpreted as molasse-type deposit derived from northern part of Capricorn Orogen. Age range constrained by Wyloo Group (below) and Bangemall Group that sandwich it.|1500-2000 Ma.||Includes basal Cherrybooka Conglomerate and Kunderong Sandstone.|Overlies Hamersley Group, Fortescue Group and Wyloo Group (all unconformably). Overlain unconformably by Bangemall Group.  Overlies Capricorn Formation unconformably.|Both matrix-supported and clast-supported boulder conglomerate; the matrix is purple, poorly sorted, micaceous granule sandstone. Gradational zone (<20m) followed by upper pebbly sandstone that dominates the Group.|
27346|Bresnahan Group|44151|6|Mentioned|p158, p160 Fig.2-146|||||||||
27346|Bresnahan Group|44867|5|Briefly described|Map Legend||Mesoproterozoic|||||||
27346|Bresnahan Group|50225|5|Briefly described|p386 Fig. 1|||||||||07-FEB-11
27346|Bresnahan Group|50226|5|Briefly described|p415, p427 Fig. 6|||Conglomerate and sandstone.  Overlies Capricorn Formation (Wyloo Group).; overlain by Edmund Group.  Age: <1.85Ga and >1.6Ga.  Geological Province: Bresnahan Basin.||||||09-DEC-04
27346|Bresnahan Group|50227|5|Briefly described|p444 Fig. 1|Mesoproterozoic|Mesoproterozoic|Age: 1600-1400Ma.||||||07-FEB-11
27346|Bresnahan Group|61262|6|Mentioned|p446 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Ashburton Basin.||||||07-NOV-08
27346|Bresnahan Group|63866|5|Briefly described|p151-p152, p154, p175|Early Mesoproterozoic|Late Palaeoproterozoic|Bresnahan Basin.||||Overlies the Wyloo and Capricorn Groups. Overlain by the Edmund Group.|Conglomerate and sandstone.|
27346|Bresnahan Group|63869|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||Unconformably overlies Wyloo Group.||
27346|Bresnahan Group|64384|5|Briefly described|p5, p48 Fig. 40|Mesoproterozoic|Mesoproterozoic|Unconformably overlies the Sylvania Inlier outcrops.||||||07-FEB-11
27346|Bresnahan Group|64580|4|Described|map legend||Paleoproterozoic|Pebble- to boulder-conglomerate, pebbly sandstone, sandstone, siltstone, and mudstone.||||||09-DEC-08
27346|Bresnahan Group|64728|6|Mentioned|p94 Fig.1, p95.|||||||Unconformably overlies Wyloo Group. Is unconformably overlain by Bangemall Supergroup.||
27346|Bresnahan Group|65506|6|Mentioned|p987 Fig.1A|||||||||
27346|Bresnahan Group|65830|5|Briefly described|p5, p13, p19; Plates 1,2|Statherian|Statherian|May correlate with the Mount Augustus Sandstone (Cooper et al. 1998). Occurs at the base of the Bangemall Supergroup.||Of the Bangemall Supergroup||Unconformably overlain by the Edmund Group.|Conglomerates.|
27346|Bresnahan Group|66299|6|Mentioned|p292.|||Northern margin of Capricorn Orogen. Siliciclastics deposited along southern margin of Pilbara Craton have large, open, west-northwesterly striking folds from Mangaroon Orogeny.||||||
27346|Bresnahan Group|67056|6|Mentioned|p419 Fig.2. |||||||||
27346|Bresnahan Group|67136|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Bresnahan Basin.||||In cross-section, overlies Ashburton Formation (Wyloo Group), and underlies Irregully Formation (Edmund Group).|Pebble to boulder conglomerate, pebbly sandstone, sandstone, siltstone and mudstone.|14-NOV-11
27346|Bresnahan Group|67855|5|Briefly described|p211, 212 fig 3-10, p224, 229|||Bresnahan Basin.||||||
27346|Bresnahan Group|68285|5|Briefly described|Map Legend|Statherian|Orosirian|Bresnahan Basin. Shown as pre-dating Mangaroon Orogeny (1677-1619 Ma, Sheppard, 2005 AJES) and post-dating the Capricorn Orogeny (1817-1722 Ma, Evans 2003, AJES) ||||Unconformably underlain by the Wyloo Group. Unconformably overlain by Irregully Formation.|Pebble- to boulder-conglomerate, pebbly sandstone, sandstone, siltstone, and mudstone (section only).|
27346|Bresnahan Group|69003|5|Briefly described|p4, p35-36|||Capricorn Orogen.||||Unconformably overlies the Wyloo Group.|A succession of coarse-grained continental to fine-grained lacustrine siliciclastic sedimentary rocks.|
27346|Bresnahan Group|69028|5|Briefly described|Map Legend|Orosirian|Orosirian|Bresnahan Basin. These two Formations are mapped as a single unit.|1800-1465 Ma.||Includes the Cherrybooka Conglomerate and the Kunderong Sandstone.||Includes pebble- to boulder-conglomerate, pebbly sandstone, sandstone, siltstone and mudstone.|15-AUG-18
27346|Bresnahan Group|69080|6|Mentioned|p684|||Pilbara Craton.|||||Conglomerate and sandstone.|
27346|Bresnahan Group|69166|5|Briefly described|geologyp_lut.csv|Mesoproterozoic|Paleoproterozoic||||||Pebble- to boulder-conglomerate, pebbly sandstone, sandstone, siltstone, and mudstone|
27346|Bresnahan Group|69185|4|Described|500k_interpgeop_pilcrat02_lut.csv|Paleoproterozoic|Paleoproterozoic|Of Bresnahan Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|||||Pebble- to boulder-conglomerate, pebbly sandstone, sandstone, siltstone, and mudstone|
27346|Bresnahan Group|69538|6|Mentioned|p517 Fig.3|||||||||
27346|Bresnahan Group|69596|5|Briefly described|p4-5, p8 Fig.5, p13|Paleoproterozoic|Paleoproterozoic|Bresnahan Basin, Capricorn Orogen.|c.1650 Ma.||||Siliciclastic sedimentary rocks.|
27346|Bresnahan Group|69745|6|Mentioned|p269|||Hamersley Province.||||Unconformably overlies Upper Wyloo Group. Is overlain by Bangemall Group.||
27346|Bresnahan Group|70327|6|Mentioned|p3|||||||||
27346|Bresnahan Group|70767|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Bresnahan Basin. Section only: no outcrop in map area.|1786-1610 Ma.|||Unconformably overlies Ashburton Formation (Wyloo Group). Is overlain unconformably by Irregully Formation (Edmund Group).|Sandstone, pebbly sandstone, pebble- to boulder- conglomerate, and siltstone.|
27346|Bresnahan Group|70768|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Bresnahan Basin. Section only: no outcrop in map area.|1786-1610 Ma.|||Unconformably overlies Ashburton Formation (Wyloo Group). Is overlain unconformably by Irregully Formation (Edmund Group).|Sandstone, pebbly sandstone, pebble- to boulder- conglomerate, and siltstone.|
27346|Bresnahan Group|70795|4|Described|100k_geologyp_lut.csv|Mesoproterozoic|Paleoproterozoic|Also 2_5m_interpgeop15_lut.csv, 100k_interpgeop_lut.csv, West Australian Craton, Bresnahan Basin|2500-1000 Ma||||Pebble to boulder conglomerate, pebbly sandstone, sandstone, siltstone and mudstone.|
27346|Bresnahan Group|70814|5|Briefly described|p8, p32, p34, p35 fig 19, p41, p74||||1786-1610 Ma|||Unconformably overlain by the Irregully Formation.||
27346|Bresnahan Group|70826|6|Mentioned|p5 tbl 2, p10|Paleoproterozoic|Paleoproterozoic|Bresnahan Basin.||||||
27346|Bresnahan Group|70958|6|Mentioned|Fig. 1|||Predominantly sandstones. Younger than Paleoproterozoic.||||||
27346|Bresnahan Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone, mudstone|
27346|Bresnahan Group|71803|6|Mentioned|p367 fig 1|||||||||
27346|Bresnahan Group|71808|6|Mentioned|p149|||||||||
27346|Bresnahan Group|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Bresnahan Basin.|||||Sandstone, pebbly sandstone, pebble- to boulder-conglomerate, and siltstone.|
27346|Bresnahan Group|72712|6|Mentioned|p3.|||Part of the Hamersley province. Overlies Mount Bruce Supergroup.||||||
27346|Bresnahan Group|73102|6|Mentioned|p20|||||||Intruded by Kulkatharra Dolerite.||
34390|Bresnahan-Mount James Supersequence|22682|5|Briefly described|Fig21,p31|Statherian|Statherian|1724-1680 Ma. Ashburton Province||||||
33103|Bridget Suite|24197|5|Briefly described|p109|Paleoproterozoic|Paleoproterozoic|Named for Bridget Adamellite and includes Parnell Quartz Monzonite. Intrudes Mosquito Creek Fm, Mount Bruce Supergroup, Warrawoona and Gorge Creek Groups. Age: 1731+/-14Ma (Rb-Sr: Collins et al, 1988). Geol. Prov: Pilbara Block.||||||07-FEB-11
33103|Bridget Suite|50287|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: c. 1803 Ma.||||||07-NOV-08
33103|Bridget Suite|50435|5|Briefly described|p2.1|Paleoproterozoic|Paleoproterozoic|Age: 1730Ma. Geological Province: Kimberley Block.||||||07-NOV-08
33103|Bridget Suite|61264|5|Briefly described|p64 Fig. 2|||Hornblende-quartz syenite to quartz monzodiorite intrusions. Geological Province: Pilbara Craton.||||||
33103|Bridget Suite|63417|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: c. 1803Ma. Hornblende monzogranite and granodiorite, micromonzonite, microsyneite and micromonzodiorite; in small stocks.||||||13-JAN-12
33103|Bridget Suite|63420|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: c.1803-1703Ma. Hornblende-feldspar-biotite porphyry dykes; trachyandesite and lamprophyre.||||||07-NOV-08
33103|Bridget Suite|63441|5|Briefly described|p13 tb. 2|Archean|Archean|Supersedes Bridget Adamellite. Age: c.1780Ma. Geological Province: Pilbara Craton.||||||07-FEB-11
33103|Bridget Suite|63854|5|Briefly described|p229 Fig.2 |Palaeoproterozoic|Palaeoproterozoic||ca. 1800 Ma|||Is overlain unconformably by Fortescue Group.|Hornblende-quartz syenite to quartz monzodiorite.|
33103|Bridget Suite|63866|4|Described|p142, p144-p145, p148|Proterozoic|Proterozoic|Eastern Pilbara Craton. Named by Budd et al., 2001 after the Bridget Adamellite of Hickman, 1978. Forms a north-northwest trending belt in the Bamboo Creek area. This suite is Sr-undepleted, Y-depleted, fractionated and shows minor alteration.|c. 1800 Ma||Includes the Parnell Quartz Monzonite.|Intrudes the Mosquito Creek Formation, Mount Bruce Supergroup, Warrawoona and Gorge Creek Groups.|Fine- to medium-grained, massive hornblende-bearing granodiorite to monzogranite.|
33103|Bridget Suite|64580|4|Described|map legend||Paleoproterozoic|Hornblende monzogranite and granodiorite, micromonzonite, microsyenite, and micromonzodiorite; in small stocks; Hornblende-feldspar-biotite porphyry dykes; trachyandesite and lamprophyre.||||||15-DEC-08
33103|Bridget Suite|64653|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Age: 1803Ma. Geological Province: Pilbara Craton. Hornblende- and biotite-bearing quartz syenite to quartz monzodiorite; fine grained, porphyritic.||||||07-FEB-11
33103|Bridget Suite|64936|5|Briefly described|map legend|Proterozoic|Proterozoic|Age: 1803-1703 Ma (geochronology: DR Nelson 2002; DR Nelson in prep). Hornblende-feldspar-biotite porphyry dykes. Geol. Prov: Pilbara Craton.||||||
33103|Bridget Suite|65008|4|Described|p5, p7, p15, p17, p18, p21, p25, p41|Orosirian|Orosirian|Named after the Bridget Adamellite (Budd et al., 2002). A sample of monzodiorite from near Granite Hill Well has a SHRIMP U-Pb zircon age of 1803 +/- 19 Ma (Nelson, 2002).|1803 +/- 19 Ma|||Intrudes the Warrawoona Group and the Mosquito Creek Formation.|Hornblende-and biotite-bearing quartz syenite to quartz monzodiorite; fine grained, porphyritic.|
33103|Bridget Suite|65726|5|Briefly described|Map legend|Proterozoic|Proterozoic||c.1803 - 1703 Ma (Nelson 2002).||||Trachyandesitic, trachytic, and lamprophyre dykes, porphyritic; hornblende monzogranite, granodiorite, micromonzonite, microsyenite, and micromonzodiorite, in small stocks.|
33103|Bridget Suite|65727|5|Briefly described|Map legend|Proterozoic|Proterozoic||c.1803 Ma.||||Hornblende monzogranite and granodiorite, micromonzonite, microsyenite and micromonzodiorite, in small stocks; hornblende-feldspar-biotite porphyry dykes, trachyandesite and lamprophyre.|
33103|Bridget Suite|65825|5|Briefly described|p6, p7 Fig.4, p24.|Paleoproterozoic|Paleoproterozoic|A NNW-trending suite of small, post-tectonic monzogranite intrusions.|1803 +/- 19 Ma (Nelson 2002c).|||Intrudes Mosquito Creek Formation.|Dominant rock type is a fine- to medium-grained, massive hornblende-bearing granodiorite to monzogranite; locally, weakly porphyritic, rounded enclaves, sparse xenoliths of metamorphosed sandstone and vein-quartz.|
33103|Bridget Suite|65827|3|Fully described|p9 Fig.3, p12 Tb.3, p14 Tb.4, p42-43|Statherian|Paleoproterozoic|Budd et al. (2002). Formerly Bridget Adamellite (Hickman, 1978). c.1803 Ma. One age is 1760 +/- 19 Ma (40Ar-39Ar; Nelson 2005). Hornblende monzogranite, granodiorite, quartz microsyenite, micromonzonite and micromonzodiorite stocks, and trachyandesite dykes. Intrudes Mount Edgar Granitic Complex, Fortescue Group, Mosquito Creek Formation, Mount Bruce Supergroup and consanguineous granitic intrusions. Includes Parnell Quartz Monzonite.||||||
33103|Bridget Suite|65828|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||c.1803 Ma (Nelson 2002).||||Medium-grained, undeformed, hornblende monzogranite in small plutons.|
33103|Bridget Suite|66217|4|Described|p6 Table 1, p55.|Statherian|Statherian|Of Budd et al. (2002); formerly Bridget Adamellite (Hickman 1978). Issues with geochronological dating of this unit are discussed.|1803 +/- 19 Ma to 1703 +/- 3 Ma.||Includes Parnell Quartz Monzonite.|Intrudes Mount Bruce Supergroup.|A series of hornblende(-clinopyroxene)-bearing stocks and bosses, from monzogranite to monzodiorite; co-magmatic with locally numerous porphyritic trachyandesite, trachyte, and lamprophyre dykes.|06-APR-16
33103|Bridget Suite|68283|5|Briefly described|Map Legend|Statherian|Statherian||c. 1803-1703 Ma||||Hornblende-feldspar-biotite porphyry dykes; trachyandesite and lamprophyre.|
33103|Bridget Suite|68981|5|Briefly described|p1, p20-21, p23, p27|||Hickman (1978). Forms a NNW-trending belt within the Pilbara Craton. A source of detrital zircons in Rudall Province. Hf evolution diagram. Crystallisation ages of a monzodiorite (Nelson, 2002) and a trondhjemitic pegmatite (Bodorkos et al., 2006) respectively. Both samples yielded xenocrystic zircon cores dated between c.3520 to c.2841 Ma indicating incorporation of east Pilbara Terrane crust.|1803+/-19 Ma; 1793+/- 17 Ma.||||Calc-alkaline, lamprophyric syenite to monzodiorite granitic rocks.|
33103|Bridget Suite|69167|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Age derived from samples of granodiorite and quartz monzonite  (142825.3.pdf, 144683.3.pdf)|1730 +/- 9 Ma  - 1760 +/- 19 Ma (Ar Isotopes)|||Intrudes Coppin Gap Granodiorite|Hornblende monzogranite and granodiorite. Hornblende-feldspar-biotite porphyry dykes; trachyandesite and lamphropyre.|
33103|Bridget Suite|69185|4|Described|500k_geologyp08_lut.csv||Paleoproterozoic|Geological Province: Pilbara Craton.|||||Hornblende monzogranite and granodiorite, micromonzonite, microsyenite, and micromonzodiorite; in small stocks; hornblende-feldspar-biotite porphyry dykes; trachyandesite and lamprophyre.|
33103|Bridget Suite|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Geological province: West Australian Craton. Events: Western Australian events. Sample GSWA 144683 (hbl-qtz monzonite) yielded an interpreted igneous crystallisation age of 2764+\-6 Ma for the monzonite; 40Ar-39Ar age of 1760+\-19 Ma is interpreted to be minimum crystallisation of the monzonite. Sample GSWA 169032 (hbl-cpx-qtz micromonzogranite) yielded an interpreted minumum igneous crystallisation age of 1703+\-4 Ma (weighted mean 40Ar-39Ar). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_geologyp08_lut.csv, 250k_interpgeol_lut.csv.|1803 Ma (isotopic)|||Intruded by Coppin Gap Granodiorite. Intrudes into Kylena Formation.|Hornblende monzogranite and granodiorite; hornblende-feldspar-biotite porphyry dykes; trachyandesite and lamprophyre.|
33103|Bridget Suite|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|Pilbara Craton.||||||
33103|Bridget Suite|71169|5|Briefly described|p59, p71-p74|Statherian|Orosirian|Pilbara Craton. Hosted by Archean rocks and occurred as volumetrically minor intraplate magamtism. Features high Sr/Y in contrast to low Sr/Y of the Kalkan Supersuite. Two Ar/Ar dates at 1674 +/- 4 Ma and 1703 +/- 6 Ma are derived from Nelson, 2004. A K-Ar date of 1674 +/- 33 Ma was also obtained (Nelson, 2002b).|1803-1674 Ma||||Calc-alkaline, felic intrusive (granitic) rocks and trachyandesite, trachyte and lamprophyre.|
33103|Bridget Suite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, granodiorite, monzonite, syenite|
33103|Bridget Suite|71795|4|Described|p45-p47|Statherian|Orosirian|East Pilbara Terrane. Date is interpreted as the magmatic age for a monzodiorite from this suite. Geochemistry is discussed briefly.|1803 +/- 19 Ma (GSWA, 2016)||||Lamprophyric syenites to monzodiorites.|
33103|Bridget Suite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic||1803+/-19 Ma.||||Hornblende monzogranite and granodiorite.|
33103|Bridget Suite|73168|5|Briefly described|p742 Fig.3, p743, p758, p764|Paleoproterozoic|Paleoproterozoic|Pilbara Craton. Capricorn Orogen.|ca 1800 Ma||||Includes monzogranitic-dioritic rocks and lamprophyric dykes. Deformed and metamorphosed.|
25810|Brigadier Formation|6876|6|Mentioned|p100 Fig.5.|Late Triassic|Late Triassic|||||||
25810|Brigadier Formation|12491|6|Mentioned|p453, p454 Fig.7.|||Deposited in a shallow sea in a pre-rift sag basin.||||Overlies Mungaroo Formation, generally conformable. Is overlain by Murat Formation.||06-NOV-14
25810|Brigadier Formation|12498|6|Mentioned|p517 Fig.3. |Early Jurassic|Early Jurassic|||||Overlies Mungaroo Formation. Is overlain by North Rankin Formation.||
25810|Brigadier Formation|23726|5|Briefly described|p8 Fig 2c|Late Triassic|Late Triassic|Overlying unit North Rankin Formation. Underlying unit Mungaroo Formation. Geological Province: Carnarvon Basin.||||||
25810|Brigadier Formation|24084|5|Briefly described|p146 Fig.2|Early Jurassic|Early Jurassic|Geological Province: North Carnarvon Basin.||||||16-MAR-05
25810|Brigadier Formation|24246|6|Mentioned|p19|||Geological Province: Carnarvon Basin.||||||
25810|Brigadier Formation|24331|5|Briefly described|p475 Fig.2|Late Triassic|Late Triassic|Conformably overlies Mungaroo Formation. Conformably overlain by Dingo Claystone. Fluvial to marginal marine. Geological Province: Barrow Sub-basin.||||||
25810|Brigadier Formation|24351|5|Briefly described|Plate 4 (in pocket)|Late Triassic|Late Triassic|Geological Province: Exmouth Plateau.||||||13-DEC-07
25810|Brigadier Formation|24390|5|Briefly described|p22|Late Jurassic|Late Triassic|Geological Province: Northern Carnarvon Basin.||||||
25810|Brigadier Formation|40617|2|Defined|p6|Early Jurassic|Late Triassic|Late Triassic to Early Jurassic.||||||01-SEP-08
25810|Brigadier Formation|40992|6|Mentioned|Fig.8|||||||||
25810|Brigadier Formation|41271|3|Fully described|p115|||||||||
25810|Brigadier Formation|41436|6|Mentioned|p44|||||||||
25810|Brigadier Formation|41440|4|Described|p136|||||||||
25810|Brigadier Formation|41732|6|Mentioned|p534|||||||||
25810|Brigadier Formation|42116|5|Briefly described|Fig.1 P6|||||||||
25810|Brigadier Formation|42615|3|Fully described|p27|Toarcian|Hettangian|Variation on Brigadier Beds. Age: Early Jurassic (late Hettangian to early Toarcian).||||||01-SEP-08
25810|Brigadier Formation|43826|6|Mentioned|Fig.2,p163|Early Jurassic|Late Triassic|||||||01-MAR-10
25810|Brigadier Formation|50085|5|Briefly described|p23 Fig. 12|Triassic|Triassic|Geological Province: Northern Carnarvon Basin.||||||
25810|Brigadier Formation|60379|6|Mentioned|p126 fig 3, p136|Rhaetian|Rhaetian|Dampier sub-basin, Carnarvon Basin||||||
25810|Brigadier Formation|60384|6|Mentioned|p244,  p243 Fig 2b|Middle Jurassic|Late Triassic|Exmouth Sub-basin, Northern Carnarvon Basin.||||||
25810|Brigadier Formation|60386|6|Mentioned|p300|Early Jurassic|Late Triassic|Northern Carnarvon Basin. Distal shelf/basin, limestone nearshore-shelf, deltaic-nearshore-shelf.||||||
25810|Brigadier Formation|61023|5|Briefly described|p27 Fig. 12|Triassic|Triassic|Geological Province: Northern Carnarvon Basin.||||||11-APR-08
25810|Brigadier Formation|62734|5|Briefly described|p1362 Fig. 2|Early Jurassic|Early Jurassic|Geological Province: Barrow Sub-basin.||||||11-APR-08
25810|Brigadier Formation|62837|5|Briefly described|Stratigraphic columns|Early Jurassic|Late Triassic|Age: ~205Ma. Geological Province: Northern Carnarvon Basin.||||||01-MAR-10
25810|Brigadier Formation|63929|6|Mentioned|p131 Fig.2.|Late Triassic|Late Triassic|Barrow Sub-basin, Peedamullah Shelf.||||Overlies Mungaroo Formation.||
25810|Brigadier Formation|63936|4|Described|p179, p184-186, p189, p191, p193|Triassic|Triassic|Originally the Brigadier Beds (Crostella and Barter, 1908) with a type section in Brigadier 1 from 3612-3964m. Formalised as Brigadier Formation by Hocking (1985) and the type section amended (Hocking, 1992) to 3620-3972m. On the basis of palynology, the unit is here redefined as the interval 3680-3923 m in Brigadier 1. This puts the top of the unit at the Triassic-Jurassic boundary (discussed). Northern Carnarvon Basin. Palynofacies and palynological zones detailed. Mainly marginal marine deposits.|||Overlies Mungaroo Formation. Is overlain unconformably by North Rankin Formation.||Shale and thinly-bedded sandstone.|
25810|Brigadier Formation|63950|5|Briefly described|p336 Fig. 4,p342-343|Early Jurassic|Late Triassic|Overlies Mingaroo Formation. Geological Province: northern Carnarvon Basin. Marine sediments in the Barrow and Dampier Sub-basins; thick, blocky sandstone thinning upwards, fining to siltstone in the latter.||||||27-MAY-08
25810|Brigadier Formation|64977|6|Mentioned|p493 Fig.3.|Late Triassic|Late Triassic|Thevenard Island area.||||||
25810|Brigadier Formation|64978|6|Mentioned|p528 Fig.2.|Early Jurassic|Late Triassic|||||||
25810|Brigadier Formation|66124|5|Briefly described|p169, p170 Fig.2||Rhaetian|Overlies Mungaroo Formation. Marginal marine. Canning Basin.||||||
25810|Brigadier Formation|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes dark grey silty? highly bioturbated, thin whisps of fine-grained sandstone; heterolithic fine-grained yellow/buff sandstone and dark grey siltstone; occasional bioturbation.|22-DEC-22
25810|Brigadier Formation|67200|5|Briefly described|p8 fig 6, p48, p49, p54, app 2 p7|Triassic|Triassic|Thermal conductivity of 1.56 W/mK||||Overlies Mungaroo Formation, overlain by North Rankin Formation|Siltstone and highly bioturbated, thin whisps of sandstone. Fine grained heterolithic sandstone and siltstone; occasional bioturbation.|
25810|Brigadier Formation|67368|5|Briefly described|p209 Fig.4, p210 Fig.5.|Early Jurassic|Late Triassic|Includes gas-bearing sands, encountered by the Lady Nora-1 well.||||Overlies Mungaroo Formation. Is overlain by North Rankin Beds.|Predominantly shales with thin sand units which are unlikely to be laterally extensive.|
25810|Brigadier Formation|67369|4|Described|p245, p246 Fig.3, pp259-262.|Rhaetian|Rhaetian|Dampier Sub-basin. Deposited in a nearshore marine setting which is described in detail; tidal bars, sandy and muddy tidal flats, estuarine beach deposits and marine shales. An estimated 103 m gross gas column was penetrated by Pluto-3 well. The change to marine conditions of this unit from the fluvial Mungaroo Formation is marked by A. reducta marker horizon.||||Overlies Mungaroo Formation. Is overlain by North Rankin Formation.|Medium-grained sandstones with shell fragments and common rip-up clasts; fine-grained sandstones with tidal varves and shell lags; dark grey heterolithic mudstones with common Teichichnus trace fossils; calcified sandstone.|
25810|Brigadier Formation|67970|5|Briefly described|p3, p7, p9, pp13-14, p25 Fig.4.|Rhaetian|Rhaetian|Hydrocarbon reservoir. Jupiter 1 (1979) well found a 22.5 m gas column in this unit. Shallow-marine to deltaic.||||Overlies Mungaroo Formation.|Marls, siltstones and thin sandstones.|
25810|Brigadier Formation|68135|5|Briefly described|p51 fig 2a|Hettangian|Rhaetian|Northern Carnarvon Basin.||||Is overlain by North Rankin Formation.||14-SEP-17
25810|Brigadier Formation|69182|6|Mentioned|Ch3 p8, Ch3 p12-p13|||Carnarvon Basin. See also Ch3 p23, Ch3 p35, Ch3 p65-p68, Ch3 p73. ||||||
25810|Brigadier Formation|69297|6|Mentioned|p336|Rhaetian|Rhaetian|Rowley Sub-basin of the Roebuck Basin. Deposited in a marine or marginal marine setting.  |||||Mudstones.|
25810|Brigadier Formation|69689|6|Mentioned|p16|Triassic|Triassic|Northern Carnarvon Basin.||||Overlies Mungaroo Formation. Is overlain by North Rankin, Bedout Formations.||
25810|Brigadier Formation|69692|5|Briefly described|p1, 3-5, 9-10, 17, 19|Triassic|Triassic|Carnarvon Basin. Biostratigraphy comprises 2 biozones and 5 subzones. Zonation diagram. Regional stratigraphic framework diagram. Six-wells correlation diagram.||||Overlies Mungaroo Formation. Is overlain by Murat Siltstone.||
25810|Brigadier Formation|70065|5|Briefly described|Regional: p4|Rhaetian|Rhaetian|Mudstone-dominated, marine to marginal marine. Encountered at the base of Huntsman 1.||||Equivalent to Bedout Formation.||
25810|Brigadier Formation|70066|5|Briefly described|Dampier:Fig.2;p1,p3. Exmouth:Fig.2;p1-2|Rhaetian|Rhaetian|See also Regional: Fig.6; p4. Northern Carnarvon Basin. Fluvio-deltaic sediments are a gas source and potential reservoirs.||||Overlies Mungaroo Formation. Is overlain by North Rankin Formation.|Thinly-bedded shelfal siltstone, claystone and marl.|
25810|Brigadier Formation|72260|5|Briefly described|p1, p3, p4, 5, 6, p7-12, 14, 16, p19-21|Early Jurassic|Rhaetian|North Carnarvon Basin. Transgressive sequence; max thickness of 1000 m; deltaic to shallow marine. Spore-pollen assemblages discussed.||||Overlies the Mungaroo Formation.|Thinly interbedded claystone and marl, and intervals of sandstone; small- to medium-scale distributary channels interbedded with siltstone, mudstone and limestone.|
25810|Brigadier Formation|73564|5|Briefly described|p1223, 1225|Triassic|Triassic|Exmouth Plateau, Gascoyne Margin.||||Overlies Mungaroo Formation. Is overlain by North Rankin Formation.|Shallow- to deep-marine clastic sediments.|
68512|Brill Monzogranite|63441|2|Defined|p46-47 Appx.1, p10 Tb. 2, p37|Archean|Archean|Of Maitland River Supersuite. Age: c.2990Ma. Geol.prov: Pilbara Craton. Monzogranite, and smaller amounts of granodiorite, foliated and locally gneissic. Medium grained, but characterised by ubquitous megacrysts of microcline; minor hornblende.||||||07-FEB-11
68512|Brill Monzogranite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Maitland River Supersuite. Geological province: Pilbara Craton.  Porphyritic monzogranite and lesser granodiorite; microcline phenocrysts; weakly foliated; metamorphosed.||||||07-NOV-08
68512|Brill Monzogranite|64580|4|Described|map legend||Mesoarchean|Of Maitland River Supersuite. Porphyritic monzogranite, and lesser granodiorite; microcline phenocrysts; weakly foliated; metamorphosed.||||||15-DEC-08
68512|Brill Monzogranite|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Maitland River Supersuite.|||Porphyritic monzogranite, and lesser granodiorite; microcline phenocrysts; weakly foliated; metamorphosed|
68512|Brill Monzogranite|70775|5|Briefly described|p53|||Together with the Jean Well Granodiorite, Whyjabby Granodiorite, Toorare Tonalite, Waloo Waloo Monzogranite and Mardeburra Granodiorite comprises the Cherratta Granitic Complex.||Maitland River Supersuite|||Coarsely microcline-porphyritic monzogranite and granodiorite, commonly containing minor hornblende.|
68512|Brill Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, granodiorite|
68512|Brill Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|De Grey Superbasin.||Maitland River Supersuite|||Porphyritic monzogranite and lesser granodiorite; microcline phenocrysts, weakly foliated; metamorphosed.|
77848|Brilliant Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2726 - 2699 Ma (inferred).|Coolgardie Subgroup|||Komatiitic basalt to high-magnesium tholeiitic basalt; thin, fine-grained, siliceous sedimentary units; rare spinifex textures; metamorphosed.|
77848|Brilliant Formation|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2726-2699 Ma (inferred)|Unit of Coolgardie Subgroup.||Intruded by Tindals Diorite.|Komatiitic basalt to high-magnesium tholeiitic basalt; thin, fine-grained, siliceous sedimentary units; rare spinifex textures; metamorphosed|
77848|Brilliant Formation|73596|6|Mentioned|p1159, 1161-1162|||Coolgardie Inlier, Kalgoorlie Terrane. Consistently mis-spelt as Brillant.||||Overlies Greenmont Basalt. Is overlain by Lindsays Basalt (Coolgardie Subgroup).||
79448|Brim Rockhole Formation|71267|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma).|1909 to 1881+\-4 Ma (inferred, isotopic)|Unit of Halls Creek Group.|||Metamorphosed carbonate (schistose or mylonitic) and siliciclastic rocks, and metamorphosed felsic and mafic volcanic rocks; includes graphitic schist, Interbedded carbonaceous pelite and psammite|
79448|Brim Rockhole Formation|71397|3|Fully described|p1,3-5,7-8,11-14,19,22-27,30,32-36|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen. Deposited in a lacustrine to shallow-marine environment. New formation name; formerly of the lower part of Biscay Formation, but redefined as a new formation based on significant differences in sedimentology and SHRIMP U-Pb zircon geochronology. Metamorphosed to upper greenschist to lower amphibolite facies. See p12 for detailed lithofacies descriptions. Contains an intercalated felsic volcanic rock dated at 1881+\-4 Ma, interpreted as age of volcanism (GA 95326012; Blake et al., 1999b). Geochemical analysis of metavolcanic rocks indicate basalt or basaltic andesite affinities. See p19, 23 for more detailed major and trace-element geochemical analysis. Metabasalts are least fractionated, and isotopicaly primitive, similar to those in Tickalara Metamorphics (interpreted to have formed in an island arc, continental back-arc or ensialic basin margin setting). Sample GSWA 206119 (metasandstone) yielded weighted mean 207Pb*/206Pb* date of 2511+\-10 Ma, interpreted as maximum depositional age. However a more robust maximum age constraint of sediment distribution is provided the underlying 1912-1904 Ma Ding Dong Downs basement. Sample GSWA 206121 (metasandstone) yielded a weighted mean 207Pb*/206Pb* date of 1909+\-10 Ma, interpreted as maximum depositional age of sandstone protolith. [Note that Kirkland et al., 2015a; 2015b GSWA 206119 and GSWA 206121 reported both samples from the lower Biscay Formation; these samples were reassigned to the Brim Rockhole Formation for the purposes of this Lamboo Province report]. Sample GA 93526012 (fragmental volcanic rock) yielded a weighted mean 207Pb*/206Pb* date of 1881+\-4 Ma, interpreted as age of volcanism. Dominated by Neoarchean to Paleoarchean detrital grains, similar to that in Saunders Creek Formation. Contains c. 1910 Ma zircons, indicating Sophie Downs Basement was exposed during Brim Rockhole deposition. See also p38,42-48.|c. 1881 Ma|Unit of Halls Creek Group.||Overlain by Biscay Formation. Underlain conformably by Saunders Creek Formation, and unconformably by Sophie Downs granite. Intruded by Woodward Dolerite.|Felsic metavolcanic and fragmental volcanic rocks, metacarbonate rocks, and planar-laminated quartzites, carbonaceous metasedimentary rocks.|
79448|Brim Rockhole Formation|71873|5|Briefly described|p427,442|Orosirian|Orosirian|Geological province: Lamboo Province. Depositional environment: lacustrine or shallow-marine. Affected by felsic volcanism at c. 1880 Ma. Intruded by Woodward Dolerite during Halls Creek Orogeny c. 1832-1808 Ma.|maximum depositional age c. 1861 Ma.|Unit of Halls Creek Group.||||
79448|Brim Rockhole Formation|73089|5|Briefly described|p25-27|||[Lamboo Province, eastern.] Range of detrital zircon age components between c. 3600 and 2500 Ma. Contains a felsic volcanic unit dated at 1881 +/- 4 Ma.||||Underlain by Saunders Creek Formation. Unconformably overlain by Biscay Formation.||
79354|Broad Arrow Subgroup|71270|5|Briefly described|100k_interpgeop_lut.csv|||Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. ||Unit of Kalgoorlie Group.|Includes Highway Formation, Scotia Basalt.|||
79354|Broad Arrow Subgroup|72095|6|Mentioned|p5 Fig 3|Neoarchean|Neoarchean|Eastern Goldfields, Yilgarn Craton.||Unit of Kalgoorlie Group.||||
79354|Broad Arrow Subgroup|73596|6|Mentioned|p1162|||Broad Arrow Inlier, Kalgoorlie Terrane.|||Scotia Basalt, Highway Formation.|Overlies Cock Robin Formation. Is overlain by Black Flag Group.||
78365|Brockman Creek kimberlite|69012|5|Briefly described|Map Legend|Orosirian|Orosirian||c. 1867 Ma (Wyatt et al., 2001)||||Kimberlite dyke.|
38756|Brooks Hill Formation|24025|5|Briefly described|p21|Cenozoic|Cenozoic|Geological Province: Pilbara Craton||||||19-NOV-08
80960|Broome, Mowla and Melligo Sandstones|72034|5|Briefly described|500k_interpgeop16_lut|Early Cretaceous|Early Cretaceous|Informal grouping of Early Cretaceous siliciclastic Canning Basin units.  Age from biostratigraphy.|||||Fine- to coarse-grained sandstone; minor mudstone and conglomerate.|
25814|Brown Gannet Limestone|13194|4|Described|p383 Tb. 4-16, p396 fig 4-60|Cretaceous|Cretaceous|Type sction Ashmore Reef 1 well (1940-2167m).100-300m thick. Name replaces Woodbine beds"".||Bathurst Island Group||Overlies Sahul Group (disconformably). Overlies Darwin Formation. Grades into Puffin Formation and Vee Formation.|Limestone and marl.|
25814|Brown Gannet Limestone|41532|2|Defined|p308|Late Cretaceous|Early Cretaceous|Reserved as Gannet Formation.||||||02-AUG-06
25814|Brown Gannet Limestone|42053|5|Briefly described|Fig.2 P29|||||||||01-MAR-10
25814|Brown Gannet Limestone|42442|2|Defined|p29|Maastrichtian|Albian|Name replaces "Woodbine Beds".||||||02-AUG-06
25814|Brown Gannet Limestone|43699|6|Mentioned|Fig.6,p10||Late Cretaceous|||||||
25814|Brown Gannet Limestone|43739|6|Mentioned|Fig.5,p38|Late Cretaceous|Early Cretaceous|||||||
25814|Brown Gannet Limestone|49637|5|Briefly described|Fig.3|Late Cretaceous|Late Cretaceous|Of the Bathurst Island Group. Geological Province: Ashmore Platform.||||||07-FEB-11
25814|Brown Gannet Limestone|70061|5|Briefly described|Regional geology Figs.6-7. Sahul: Fig.2|Santonian|Coniacian|See also Vulcan: Fig.2.||Bathurst Island Group.||Overlies Woolaston Formation. Is ovelain by Fenelon Formation.||12-JUL-16
25814|Brown Gannet Limestone|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Santonian|Coniacian|See also Northern: Fig.2. Yampi: Fig.2. Browse Basin. Not present in Yampi and Leveque Shelves.||Bathurst Island Group.||Overlies Woolaston Formation. Is overlain by Fenelon Formation.||12-JUL-16
23427|Brownrigg Sandstone|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Of Tarcunyah Group, Officer Basin.||||||
23427|Brownrigg Sandstone|23590|3|Fully described|p13|||Of Tarcunyah Group. Overlying unit Yandanunyah Formation. Geological Province: Officer Basin. Max. thickness: >600 m.||||||
23427|Brownrigg Sandstone|23594|4|Described|p22|Neoproterozoic|Mesoproterozoic|Of Tarcunyah Group. Overlying unit Yandanunyah Formation. Underlying unit Waroongunyah Formation. Bangemall Basin. Max. thickness: >400 m.||||||
23427|Brownrigg Sandstone|23729|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Tarcunyah Group. Geological Province: Paterson Orogen||||||
23427|Brownrigg Sandstone|23730|4|Described|p11|Neoproterozoic|Neoproterozoic|Of Tarcunyah Group. Overlying unit Wongarlong Formation.  Geological Province: Officer Basin.||||||
23427|Brownrigg Sandstone|23746|4|Described|p26|Neoproterozoic|Mesoproterozoic|Of Tarcunyah Group.||||||
23427|Brownrigg Sandstone|23760|4|Described|p28|Proterozoic|Proterozoic|Of Tarcunyah Group. Geological Province: Officer Basin.||||||
23427|Brownrigg Sandstone|24025|5|Briefly described|p16|Neoproterozoic|Neoproterozoic|Of the Tarcunyah Group.  Geological Province: Officer Basin.||||||
23427|Brownrigg Sandstone|41669|2|Defined|Table 5|Precambrian?||||||||
23427|Brownrigg Sandstone|42352|6|Mentioned|p29|||Part of Yeneena Group||||||
23427|Brownrigg Sandstone|43055|4|Described|p28, Table 4|||of Yeneena Group||||||
23427|Brownrigg Sandstone|43056|5|Briefly described|Map Legend|||of Yeneena Group||||||
23427|Brownrigg Sandstone|43847|5|Briefly described|Map Legend||Proterozoic|||||||17-FEB-10
23427|Brownrigg Sandstone|44139|5|Briefly described|p277-280|Neoproterozoic|Neoproterozoic|Williams (1989). 350 m. Sandstone. Western zone of Yeneena Basin.| | ||||05-MAR-18
23427|Brownrigg Sandstone|44190|5|Briefly described|Map Legend||Proterozoic|||||||
23427|Brownrigg Sandstone|44831|5|Briefly described|Map Legend||Proterozoic|||||||
23427|Brownrigg Sandstone|50008|5|Briefly described|p46 Fig.3||Neoproterozoic|Of Tarcunyah Group. Geological Province: Officer Basin.||||||
23427|Brownrigg Sandstone|60470|5|Briefly described|p4 Fig. 2|Neoproterozoic|Neoproterozoic|in Officer Basin, of Tarcunyah Group. Sandstone; minor conglomerate, siltstone, and shale||||||
23427|Brownrigg Sandstone|62453|4|Described|p66|Cryogenian|Cryogenian|Of the Tarcunyah Group. Thickness: 600m. Geological Province: Paterson Orogen. Sandstone. ||||||
23427|Brownrigg Sandstone|64580|6|Mentioned|map legend|||Of Tarcunyah Group.||||||15-DEC-08
23427|Brownrigg Sandstone|64777|5|Briefly described|p3 Fig.4 |Neoproterozoic|Neoproterozoic|||Of the Tarcunyah Group|||Sandstone; minor conglomerate, siltstone and shale.|
23427|Brownrigg Sandstone|65454|4|Described|p7 Fig.3, p10, p30 Fig.A1b|Cryogenian|Cryogenian|Of Tarcunyah Group. Fine- to coarse-grained quartz sandstone with minor interbedded carbonate siltstone. Overlies Waroongunyah Formation. Overlain by Yandanunyah Formation.||||||
23427|Brownrigg Sandstone|65725|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Tarcunyah Group. Underlain by Waroongunyah Formation. Overlain by Yandanunyah Formation. Fine- to coarse-grained quartz sandstone. Contains pyrite nodules. Province: Officer Basin (Centralian Superbasin)||||||26-FEB-13
23427|Brownrigg Sandstone|65826|5|Briefly described|p1, p11. |Neoproterozoic|Neoproterozoic|||Unit in Tarcunyah Group.||Is overlain conformably by Yandanunyah Formation.|White, cream to light brown, fine- to coarse-grained quartz sandstone with cubic and spherical voids after pyrite and limonite; scattered small pebbles of vein quartz; well-bedded, flaggy; cross-lamination, ripple marks and current striae common.|
23427|Brownrigg Sandstone|67202|4|Described|p64-65, p231|Neoproterozoic|Neoproterozoic|NW Officer Basin. 400m thick. Shallow-marine shelf deposits. See also Brownrigg Formation (p117).||Tarcunyah Group.||Conformably overlies Waroongunyah Formation. Is overlain conformably by Yandanunyah Formation.|Fine- to coarse-grained sandstone and orthoquartzite.|15-FEB-18
23427|Brownrigg Sandstone|69167|4|Described|geologyp_lut.csv|Neoproterozoic|Neoproterozoic|||Tarcunyah Group|||Quartz sandstone, fine to coarse grained, moderately to well sorted, flaggy to cross-bedded; scattered pebbles of vein quartz.|
23427|Brownrigg Sandstone|69185|5|Briefly described|500k_geologyp08_lut.csv|Neoproterozoic|Neoproterozoic|||Unit of Tarcunyah Group.||||
23427|Brownrigg Sandstone|69590|4|Described|GEOL_LUT_CSV files|Cryogenian|Neoproterozoic|Of Gibson Sub-basin, Officer Basin (Phase 1), Centralian Superbasin. Events: Mosquito Creek Orogeny; North Pilbara Orogeny; Prinsep Orogeny; East Pilbara Terrane Rifting Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|1000-635 Ma (Inferred)|Unit of Tarcunyah Group.|||Quartz sandstone, fine to coarse grained, moderately to well sorted, flaggy to cross-bedded; scattered pebbles of vein quartz|
23427|Brownrigg Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Cryogenian|Tonian|Gibson Sub-basin, Officer Basin (Phase 1).||Tarcunyah Group|||Quartz sandstone, fine to coarse grained, moderately to well sorted, flaggy to cross-bedded; scattered pebbles of vein quartz.|
30280|Browns Range Metamorphics|22496|6|Mentioned|p9||Neoarchean|||||||07-NOV-08
30280|Browns Range Metamorphics|23621|2|Defined|p51 Appendix|Archean|Archean|See also page 13, page 12 table 1. Previously mapped as undivided Halls Creek Group and Tanami Complex. Age: 2507+/-22 Ma. Overlying unit Gardiner Sandstone (unconformably). Browns Range Dome. Max. thickness: >1000 m.||||||07-NOV-08
30280|Browns Range Metamorphics|23622|5|Briefly described|Map Legend|Paleoproterozoic|Archean|Geological Province: Browns Range Dome.||||||07-NOV-08
30280|Browns Range Metamorphics|23809|6|Mentioned|p2, p3 Fig. 1|||In the Tanami region.||||||
30280|Browns Range Metamorphics|43301|5|Briefly described|Map Legend||Archean|Metamorphosed at 2504+/-4 Ma.||||||07-NOV-08
30280|Browns Range Metamorphics|50315|5|Briefly described|Map Legend|Archean|Archean|Undifferentiated schist, gneiss, migmatite; undifferentiated Archaean: felsic and mafic gneiss, granites and migmatite.||||||07-NOV-08
30280|Browns Range Metamorphics|50374|5|Briefly described|Map Legend|Archean|Archean|||||||07-NOV-08
30280|Browns Range Metamorphics|50376|5|Briefly described|Map Legend|Archean|Archean|Undifferentiated schist, gneiss, migmatite; undifferentiated Archaean - felsic and mafic gneiss, granite and migmatite.||||||07-NOV-08
30280|Browns Range Metamorphics|60676|5|Briefly described|Map legend|Archean|Archean|Underlies MacFarlane Peak Group. Undifferentiated schist, gneiss, migmatite; undifferentiated Archaean: felsic and mafic gneiss, granite and migmatite.||||||07-NOV-08
30280|Browns Range Metamorphics|61861|4|Described|p3 Table 1, p5, p23, Map 1|Neoarchean|Neoarchean|New name; applied to 1 - 3 km thick high grade metamorphics confined to a narrow fault-bound slice with high magnetic response on southern margin of Browns Range Dome. Gneiss metamorphosed 1882 +/- 14 Ma.|2505 +/- 4 Ma enclaves in 2510 +/- 22 Ma granite.|||Unconformably overlain by Birrindudu Group|Includes granitic gneiss and muscovite schist intruded by fine-grained granite, thin granite sills, aplite and pegmatite.|03-APR-12
30280|Browns Range Metamorphics|62580|6|Mentioned|p8, p12 Fig. 2|Archean|Archean|||||||07-FEB-11
30280|Browns Range Metamorphics|63261|5|Briefly described|p7, p9, p17|||Of Blake et al (2000) for metamorph'd arkosic sed.rocks exposed near Browns Range granite complex in WA. Include quartzofeldspathic gneiss+muscovite schist intruded by aplite+ pegmatite.See also informal Browns Range metamorphics.Age discussion included||||||10-DEC-12
30280|Browns Range Metamorphics|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Metamorphosed feldspathic siliciclastic rocks, minor calc-silicate rock; meta-ultramafic rock; amphibolite to granulite facies.||||||15-DEC-08
30280|Browns Range Metamorphics|64675|5|Briefly described|Fig.7(a-b), Map 4, p14, Fig.20-22|Archean|Archean||1882 Ma|Of the Coomarie Suite.||Unconformably overlain by the Gardiner Sandstone of the Birrindudu Group. Unconformably overlain by the MacFarlane Peak Group.|Comprises granitic orthogneiss, muscovite paragneiss and schist.|19-MAR-14
30280|Browns Range Metamorphics|65323|5|Briefly described|Map legend|Archean|Archean|Most units not present on map; undifferentiated non-magnetic schist, gneiss, migmatite.||||||13-NOV-15
30280|Browns Range Metamorphics|65324|6|Mentioned|Map legend|Archean|Archean|Not shown on map||||||
30280|Browns Range Metamorphics|65326|6|Mentioned|Map legend|Archean|Archean|Not shown on map||||||02-FEB-10
30280|Browns Range Metamorphics|65327|5|Briefly described|Map legend|Archean|Archean|Felsic and mafic gneiss, granite and migmatite informally subdivided based on variations in magnetic and gravity response; 3 (of 4) units are shown on this sheet and have high gravity and non-, variably, or moderate-intensely magnetic response||||||
30280|Browns Range Metamorphics|65328|5|Briefly described|Map legend|Archean|Archean|Felsic and mafic gneiss, granite and migmatite informally subdivided based on variations in magnetic and gravity response; 3 (of 4) units are shown on this sheet and have high gravity and non-, variably, or moderate-intensely magnetic response||||||02-FEB-10
30280|Browns Range Metamorphics|65349|6|Mentioned|Map legend|Archean|Archean|Not shown on map||||||
30280|Browns Range Metamorphics|65350|6|Mentioned|Map legend|Archean|Archean|Not shown on map||||||
30280|Browns Range Metamorphics|65351|6|Mentioned|Map legend|Archean|Archean|Not shown on map||||||
30280|Browns Range Metamorphics|65352|6|Mentioned|Map legend|Archean|Archean|Not shown on map||||||
30280|Browns Range Metamorphics|65353|6|Mentioned|Map legend|Archean|Archean|Not shown on map||||||
30280|Browns Range Metamorphics|65354|6|Mentioned|Map legend|Archean|Archean|Not shown on map||||||
30280|Browns Range Metamorphics|65355|6|Mentioned|Map legend|Archean|Archean|Not shown on map||||||
30280|Browns Range Metamorphics|65356|6|Mentioned|Map legend|Archean|Archean|Not shown on map||||||
30280|Browns Range Metamorphics|67127|5|Briefly described|p175|Palaeoproterozoic|Archaean|Tanami-region. Intruded by an unnamed granitic core.|||||Meta-arkose, feldspathic metasandstone and schist.|
30280|Browns Range Metamorphics|67168|5|Briefly described|Map legend.|Archean|Archean|Areas with different magnetic and gravity responses are mapped separately.||||Unconformably overlain by MacFarlane Peak Group.|Felsic and mafic gneiss, granite, migmatite.|
30280|Browns Range Metamorphics|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleoproterozoic|Paleoproterozoic|See also 100k_maginterpgeop_lut.csv and 500k_geologyp08_lut.csv. Granites-Tanami Complex. Non-magnetic.|c.2510 Ma (Page et al., 1995).||||Feldspathic psammite and subordinate psephite; amphibolite to granulite facies.|25-NOV-15
30280|Browns Range Metamorphics|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|||||Feldspathic psammite and subordinate psephite; amphibolite to granulite facies.|30-JUL-15
30280|Browns Range Metamorphics|69165|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Metamorphosed feldspathic siliciclastic rocks, minor calc-silicate rock; meta-ultramafic rock; amphibolite to granulite facies.|
30280|Browns Range Metamorphics|69419|5|Briefly described|p4:7,|Paleoproterozoic|Paleoproterozoic|Forms a crescent-shaped belt along the S edge of Browns Range Inlier (previously the Browns Range Dome). Previous interpretations of an Archean age (2510 +/- 22 Ma; Page et al., 1995) were probably based on inherited zircons.|||||Granite, gneiss and metamorphic rocks.|12-JUL-16
30280|Browns Range Metamorphics|69426|5|Briefly described|p11:3-5, 10-11|||Crops out along the S and W margins of Browns Range Dome. Over 3000m thick. Parts of this unit are possibly lateral equivalents of the Dead Bullock Formation. Maximum detrital zircon depositional age. A SHRIMP U-Pb zircon age of 2510 +/- 22 Ma (Page et al., 1995) for the protolith is probably (Cross and Crispe, 2007) from an inherited sedimentary source, as also with zircons from a leucogranite dated at c.1970 Ma and 1882 Ma.|<2507 +/- 22 Ma (Page et al., 1995).||||Quartzofeldspathic gneiss, muscovite schist, fine-grained granite, aplite, pegmatite, and metamorphosed arkosic sandstone.|12-JUL-16
30280|Browns Range Metamorphics|69432|6|Mentioned|p17:4|||Tanami Region.||||||12-JUL-16
30280|Browns Range Metamorphics|69587|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Granites-Tanami Orogen, North Australian Craton. Events: Alice Springs Orogeny; Tanami Orogeny D1t. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|1874-1838 Ma (inferred)||||Feldspathic psammite and subordinate psephite; amphibolite to granulite facies|
30280|Browns Range Metamorphics|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Granites-Tanami Orogen. Events: Alice Springs Orogeny; Tanami Orogeny D1t. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|1874-1838 Ma (Isotopic)||||Metamorphosed feldspathic siliciclastic rocks, minor calc-silicate rock; meta-ultramafic rock; amphibolite to granulite facies|
30280|Browns Range Metamorphics|70141|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|1874-1838 Ma.||||Feldspathic psammite and subordinate psephite; amphibolite to granulite facies.|
30280|Browns Range Metamorphics|70154|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 100k_interpgeop_lut.csv. |1838-1874 Ma||||Feldspathic psammite and subordinate psephite; amphibolite to granulite facies|
30280|Browns Range Metamorphics|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|Aileron Province [?].||||||15-MAY-20
30280|Browns Range Metamorphics|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Granites-Tanami Orogen. Events: Alice Springs Orogeny (450-295 Ma); Stafford Event (1810-1790 Ma); Tanami Event (1850-1830 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv and geochron files.|1874+\-10 to 1838+\-6 Ma (isotopic)|||Overlain unconfomably by Gairdiner Sandstone/Birrindudu Group.|Feldspathic psammite and subordinate psephite; amphibolite to granulite facies; quartzofeldspathic granofels with sparse to abundant pebbles and cobbles; minor banded ironstone, siltstone, and foliated conglomeratic calc-silicate rocks|
30280|Browns Range Metamorphics|71349|5|Briefly described|p723-739|Archean|Archean|Tanami Region, North Australian Craton. Abbreviated to BRM throughout the article. Immature to sub-mature, meta-arkosic rocks with minor quantities of granitic lithic fragments. Lithology elaborated; photographs, photomicrographs. Geochemistry, zircon analyses detailed. Age range from detrital zircon maximum depositional age and age of granite intrusions.|3026 +/- 11 Ma - c.2.5 Ga.|||Is overlain unconformably by Dead Bullock Formation and Gardiner Sandstone.|Mainly metasandstones, occasional interbedded medium- to coarse-grained conglomerates, and less common calc-silicate rocks and BIF. Cut by numerous felsic and mafic-ultramafic intrusions.|
30280|Browns Range Metamorphics|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen|Max age 1874+/-10 Ma, min age 1838+/-6 Ma.||||Feldspathic psammite and subordinate psephite; amphibolite to granulite facies.|
30280|Browns Range Metamorphics|72071|4|Described|p1297-1299,1301-1304|Archean|Archean|Crops out over an area of ~100 km2. Clastic detritus sourced from erosion of Mesoarchean granitic source. Experienced greenschist metamorphism at ca. 1.83 Ga (Crispe et al., 2007). Intruded by minor ca. 2.5 Ga granitic to pegmatitic intrusions and mafic-ultramafic rocks that were affected by regional metamorphism that predate ca. 1.83 Ga metamorphic activity.|3.1-2.5 Ga|||Overlain unconformably by Birrindudu Group. Intruded by Browns range dome granite.|Immature quartz-feldspar meta-arkosic sandstones, with minor interbedded conglomerates and semipelitic schists.|01-JUL-19
30280|Browns Range Metamorphics|73089|4|Described|p3, p5-7, p29-30|Paleoproterozoic|Mesoarchean|Exposed in the western and southern margins of the Browns Range Dome. Proposed as a Neoarchean basement inlier. Interpretation of zircon dates remains the subject of debate; inferred depositional ages ranging from Mesoarchean-Neoarchean to Paleoproterozoic. Some authors suggest the c. 2500 Ma population is inherited; thus, the unit could be correlative with Dead Bullock Formation. [Authors equate this unit to the Kairos member as part of the Tanamai Group]. Unconformably overlain by sedimentary rocks of the Paleoproterozoic to Mesoproterozoic Birrindudu Basin.|1885-1865 Ma? 3000-2500 Ma?|||Unconformably overlain by Gardiner Sandstone.|Feldspathic metasandstone, metaconglomerate and muscovite schist, with less common calc-silicate rock and banded iron formation.|
30280|Browns Range Metamorphics|73158|6|Mentioned|p2, p9|||Granites-Tanami Orogen, northwest.|||||Granitic gneisses.|
30280|Browns Range Metamorphics|73159|5|Briefly described|p2, 9|Archaean|Archaean|Northwest Granites-Tanami Orogen.|||||Granitic gneisses.|
29869|Bryah Group|12099|4|Described|p676-8, 680-1, 684-6, Figs.1, 2, 4,5,8|Orosirian|Orosirian|New or redefined unit by Occhipinti et al. (1997). Mostly made up by Narracoota Formation. Age poorly constrained; max depositional age given by detrital zircons in Ravelstone Formation dated at 2014+/-22 Ma (Nelson, 1997). Minimum age given by Pb-Pb isochron age of 1920+/-35 Ma from the Narracoota Formation. Hosts orogenic Au mineralisation. Volcanic rocks of Bryah Group have an oceanic affinity deposited in a backarc rift setting.|Between 2000 and 1920 Ma.||Includes Karalundi, Narracoota, Horseshoe and Ravelstone Formations.|In tectonic contact with Peak Hill Schist and Padbury Group. Locally unconformably overlain by Padbury Group. Thrust over the Yerrida Group along the Goodin Fault.||04-MAR-13
29869|Bryah Group|22501|6|Mentioned|p117|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
29869|Bryah Group|22694|4|Described|p7|||Glengarry Basin||||||
29869|Bryah Group|22695|5|Briefly described|map|Proterozoic|Proterozoic|||||||
29869|Bryah Group|22696|5|Briefly described|map|Proterozoic|Proterozoic|||||||
29869|Bryah Group|22697|5|Briefly described|map|Proterozoic|Proterozoic|||||||
29869|Bryah Group|22698|5|Briefly described|map|Proterozoic|Proterozoic|||||||
29869|Bryah Group|22716|6|Mentioned|table4, p234,229|Paleoproterozoic|Paleoproterozoic|Deposited in the Bryah rift.||||||07-NOV-08
29869|Bryah Group|22940|4|Described|p13, Fig.1 p3, Fig.6 p14|Paleoproterozoic|Paleoproterozoic|See also Table 2 p12. In the Bryah Basin.||||||07-NOV-08
29869|Bryah Group|23151|5|Briefly described|p64|||||||||
29869|Bryah Group|23153|5|Briefly described|p83|||In the Bryah Basin.||||||23-JAN-08
29869|Bryah Group|23485|6|Mentioned|p4 Fig. 2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
29869|Bryah Group|23525|5|Briefly described|p2 Fig. 1||Orosirian|Age: <2000Ma||||||
29869|Bryah Group|23586|5|Briefly described|p15|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
29869|Bryah Group|23589|5|Briefly described|p20|||Overlain by Earaheedy Group.||||||23-JAN-08
29869|Bryah Group|23592|4|Described|p10|Paleoproterozoic|Paleoproterozoic|Overlain by Padbury Group. Geological Province: Bryah Basin.||||||07-NOV-08
29869|Bryah Group|23593|5|Briefly described|p2 Fig 1|||Overlain by Padbury Group. Underlain by Yerrida Group. Geological Province: Bryah Group.||||||23-JAN-08
29869|Bryah Group|23597|6|Mentioned|p8|||||||||
29869|Bryah Group|23600|5|Briefly described|p4 Fig 2|||Geological Province: Bryah Basin.||||||
29869|Bryah Group|23744|4|Described|p11|Paleoproterozoic|Paleoproterozoic|Geological Province: Bryah Basin.||||||07-NOV-08
29869|Bryah Group|23747|4|Described|p9|Paleoproterozoic|Paleoproterozoic|Geological Province: Bryah Basin.||||||07-NOV-08
29869|Bryah Group|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Bryah Basin||||||
29869|Bryah Group|23749|4|Described|p11|Proterozoic|Proterozoic|Geological Province: Bryah Basin.||||||
29869|Bryah Group|23750|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Bryah Basin.||||||
29869|Bryah Group|23759|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
29869|Bryah Group|23781|5|Briefly described|p27 Fig. 10||Paleoproterozoic|||||||07-NOV-08
29869|Bryah Group|23798|5|Briefly described|p2|||Includes Narracoota Volcanics and Thaduna Greywacke. Geological Province: Yilgarn Craton.||||||05-JUL-06
29869|Bryah Group|23865|6|Mentioned|p170 Fig.1|||Geological Province: Yilgarn Craton.||||||
29869|Bryah Group|23890|5|Briefly described|p21 Fig.11|||Geological Province: Bryah Basin.||||||
29869|Bryah Group|24017|5|Briefly described|p8 Tb. 2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
29869|Bryah Group|24021|5|Briefly described|p3, Fig. 1|||||||||
29869|Bryah Group|24028|5|Briefly described|p288 Fig. 1|||||||||
29869|Bryah Group|24183|5|Briefly described|p2 Fig.1, p20|Mesoproterozoic|Mesoproterozoic|Unconformably overlain by the Collier Group.||||||
29869|Bryah Group|24332|5|Briefly described|p135 Fig. 1|Paleoproterozoic|Paleoproterozoic|Volcanic and sedimentary rocks. Age: c.2000Ma.||||||07-NOV-08
29869|Bryah Group|24535|5|Briefly described|p22, 23|Paleoproterozoic|Paleoproterozoic|Thrust over Yerrida Group.||||||26-NOV-13
29869|Bryah Group|24544|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Age: <2000 Ma. Previously of the "Glengarry Group".||||||07-NOV-08
29869|Bryah Group|43238|4|Described|p6|||||||||
29869|Bryah Group|43831|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
29869|Bryah Group|44204|5|Briefly described|Map Legend||Proterozoic|||||||
29869|Bryah Group|44867|5|Briefly described|Map Legend||Mesoproterozoic|||||||
29869|Bryah Group|44927|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
29869|Bryah Group|49893|5|Briefly described|p2 Fig.1|Proterozoic|Proterozoic|Contains units formerly in the Glengarry Group.||||||
29869|Bryah Group|49896|5|Briefly described|p3 Tb. 2, p6|||Along with the Yerrida Group, supersedes the Glengarry Group. Comprises Karalundi, Narracoota and Horseshoe Formations, as well as the newly defined Ravelstone Formation. Geological Province: Glengarry Basin.||||||
29869|Bryah Group|50218|5|Briefly described|p238 Fig. 1, p244, p242 Fig. 4.|Paleoproterozoic|Paleoproterozoic|Contains metamorphosed and poly-deformed siliciclastic and chemical sedimentary rocks, together with voluminous mafic to ultramafic rocks and minor intrusive rocks. Overlies Padbury Group. Age: <2000Ma. Geol. Prov: Bryah Basin.||||||07-FEB-11
29869|Bryah Group|50219|5|Briefly described|p258 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: <2000Ma.||||||07-FEB-11
29869|Bryah Group|50221|5|Briefly described|p296 Fig.1, p297|Mesoproterozoic|Paleoproterozoic|Overlain by Padbury Group. Age: <2000 Ma. Geological Province: Bryah Basin.||||||07-NOV-08
29869|Bryah Group|50222|4|Described|p320 Fig. 3, p324|Paleoproterozoic|Paleoproterozoic|Includes the Karalundi, Narracoota, Ravelstone and Horseshoe Formations.   Geological Province: Bryah Basin.  See also p319 Fig. 2.||||||07-NOV-08
29869|Bryah Group|50225|5|Briefly described|p386 Fig. 1|||||||||07-FEB-11
29869|Bryah Group|50226|5|Briefly described|p420|||Divided into the Karalundi, Narracoota, Ravelstone and Horseshoe formations.  Geological Province: Bryah Basin.||||||24-JUN-04
29869|Bryah Group|61217|5|Briefly described|p42 Fig., p45|Proterozoic|Proterozoic|Includes Narracoota and Peak Hill Formations.||||||07-FEB-11
29869|Bryah Group|61269|6|Mentioned|p86 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
29869|Bryah Group|61271|6|Mentioned|p104|||||||||
29869|Bryah Group|62289|5|Briefly described|plate 1, p3 Fig. 1|Palaeoproterozoic|Palaeoproterozoic|Includes Narracoota and Karalundi Formations. Geol. Prov: Bryah Basin.||||||
29869|Bryah Group|63866|5|Briefly described|p152, p162, p164-p165, p168, p175||Orosirian|Western Glengarry Basin. Maximum age is constrained by a SHRIMP U-Pb age for detrital zircons in the Ravelstone Formation. |||Includes the Karalundi, Narracoota, Ravelstone and Horseshoe Formations.|Unconformably overlain by the Collier Group and the Mount Leake Formation. Faulted against the Padbury Group.||
29869|Bryah Group|64580|6|Mentioned|map legend|||||||||
29869|Bryah Group|64724|4|Described|p43, 46|Orosirian|Orosirian|Clastic and chemical sediments.|||Contains Ravelstone Formation and Horseshoe Formation.|Overlain by Padbury Group.||02-APR-12
29869|Bryah Group|64725|5|Briefly described|p64.|Paleoproterozoic|Paleoproterozoic|West Australian Craton. Contains amagmatic orogenic, shear zone-hosted, Au lodes.||||||
29869|Bryah Group|64728|6|Mentioned|p94 Fig.1. |Paleoproterozoic|Paleoproterozoic|||||Is unconformably overlain by Bangemall Supergroup.||
29869|Bryah Group|65408|5|Briefly described|pp81 - 85.|Statherian|Orosirian|Pb/Pb model age: 1.7 Ga of pyrite formed in late stage gold mineralization, Narracoota Formation.|1920 +/- 35 Ma Pb/Pb model age, Narracoota Fm||Includes Karalundi, Narracoota, Ravelstone and Horseshoe Formations.|Thrust over Yerrida Group.Everywhere in fault contact with Yerrida Group rocks. Is unconformably overlain by Padbury Group.|Includes a sequence of greywacke and conglomerate; mafic-ultramafic volcanic rocks; turbiditic sedimentary rocks; chemical and fine-grained clastic units.|21-JAN-22
29869|Bryah Group|65411|5|Briefly described|p88, p89 Fig.1, p91, p94.|Paleoproterozoic|Paleoproterozoic|Bryah Basin. Rocks of this unit and Yerrida Group were formerly of the Glengarry Group (abandoned). Lower parts are tectonically interleaved with Padbury Group.|||Includes Karalundi, Narracoota, Ravelstone and Horseshoe Formations.|Is overlain unconformably by Padbury Group.||
29869|Bryah Group|65412|5|Briefly described|pp96-103.|Paleoproterozoic|Paleoproterozoic||||Includes Karalundi and Narracoota Formations.|||
29869|Bryah Group|65419|2|Defined|pp1-2, p4 Fig.1, p6, p27, pp29-37.|Paleoproterozoic|Paleoproterozoic|Bryah Basin. Named after Bryah Homestead. Rocks of this unit were formerly included in the Glengarry Group of Gee (1979, 1987) and Gee and Grey (1993) in the (western) Glengarry Basin, both terms now obsolete. Pirajno and Occhipinti (1995) also included the Peak Hill and Labouchere Formations, but this study no longer includes them.|2014 +/- 22 Ma (max. deposition; Nelson, 1997).||Includes Karalundi, Narracoota, Horseshoe and Ravelstone Formations.|Is in faulted contact with Peak Hill Schist and Yerrida Group. Is unconformably overlain by Mount Leake Formation and by the Bangemall Group.|Mafic and ultramafic extrusive and intrusive rocks, metabasite, terrigenous clastic rocks, and wacke.|
29869|Bryah Group|65472|6|Mentioned|p1|||Bryah Basin. May be overlain by Earaheedy Basin.||||||24-SEP-15
29869|Bryah Group|65896|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Bryah Basin. 2014 - 1920 Ma. Includes Narracoota, Ravelstone and Horseshoe Formations.||||||
29869|Bryah Group|65913|6|Mentioned|p2 Fig.1, p3.||||||Includes Karalundi, Narracoota, Horseshoe and Ravelstone Formations.|||24-MAY-16
29869|Bryah Group|66112|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Bryah Basin. Includes Narracoota, Ravelstone and Horseshoe Formations, as well as mapped but unnamed units of schists, chert, dolerite, siltstone and basalt.||||||
29869|Bryah Group|66299|6|Mentioned|p57, p148, p208.|||Formerly part of Glengarry Group (Daniels 1975). Once thought to be equivalent to metasediments of Moogie Metamorphics.|||Includes Narracoota Formation.|||
29869|Bryah Group|66427|6|Mentioned|p41 Tb.1, p42 ||||||Includes Narracoota and Ravelstone Formations.|Is overlain by Padbury Group.||
29869|Bryah Group|67843|6|Mentioned|p2 Fig.1. |Proterozoic|Proterozoic|||||||
29869|Bryah Group|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic|also used in 2_5M_GEOLOLYP98_LUT|||Includes Horseshoe Formation, Karalundi Formation, Narracoota Formation, Ravelstone Formation.|||
29869|Bryah Group|69003|5|Briefly described|p4, p12-13|||Bryah Basin, Capricorn Orogen. Hosts VHMS base-metal deposits at Doolgunna.|||Karalundi, Narracoota, Ravelstone, Horseshoe Formations.|||
29869|Bryah Group|69010|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Bryah Basin.|||Includes Horseshoe Formation, Ravelstone Formation, and Narracoota Formation.|||
29869|Bryah Group|69028|5|Briefly described|Map Legend|Orosirian|Paleoproterozoic|Bryah Basin.|||Includes Narracoota and Ravelstone Formations.||Includes metabasalt and mafic-ultramafic schist; locally pillowed and plagioclase-phyric; interbedded with volcaniclastic and sedimentary rock.|14-SEP-15
29869|Bryah Group|69080|6|Mentioned|p684|||Yilgarn Craton.|||||Turbiditic sandstone and siltstone with minor iron-formation overlying intrusive and volcaniclastic metamafic and meta-ultramafic rock.|
29869|Bryah Group|69166|6|Mentioned|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic||||Includes Horseshoe Formation, Narracoota Formation, Ravelstone Formation, Karalundi Formation|||
29869|Bryah Group|69313|6|Mentioned|p19|||Padbury Foreland Basin. ||||||
29869|Bryah Group|69387|6|Mentioned|p11|||Narryer Terrane.||||||
29869|Bryah Group|69583|5|Briefly described|Plate 2|Proterozoic|Proterozoic|Bryah Basin.|||Horseshoe, Narracoota Formations.|||
29869|Bryah Group|69596|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Capricorn Orogen.||||||
29869|Bryah Group|70795|6|Mentioned|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 2_5m_interpgeop15_lut.csv, West Australian Craton, Bryah Basin|2014-1920 Ma||Includes Horseshoe Formation, Ravelstone Formation, Narracoota Formation||Turbiditic sandstone and siltstone with minor iron formation, basalt, felsic volcanic, ultramafic and siliciclastic sedimentary rocks.|
29869|Bryah Group|70796|6|Mentioned|2_5m_interpgeop15_lut.csv|Paleoproterozoic|Paleoproterozoic|Of the Bryah Basin, Capricorn Orogen. Affected by the following events: Capricorn Orogeny (1817  1772 Ma); Glenburgh Orogeny (2002  1947 Ma). See also 500k_interpgeop14_lut.csv, glengarry_100l_geologyp_lut.csv, glengarry_500k_interpgeop_lut.csv, Glengarry100_2645_stratig.pdf.|||Subdivided into an upper and lower part.|||
29869|Bryah Group|70804|4|Described|p1-p7, p14, p17-p18, p21|Statherian|Orosirian|Together with the Padbury Group makes up the western part of the former 'Glengarry Basin'. Gold and minerals production and remaining resources detailed. See also p22-p34, p37-p38, p42, p44-p45.|c. 2000-1800 Ma||Includes the Karalundi Formation, Narracoota Formation, Ravelstone Formation, Horseshoe Formation.|Faulted against the Yerrida Group and Peak Hill Schist. Unconformably overlain by the Padbury Group.||
29869|Bryah Group|70814|5|Briefly described|p15, p26, p40, p48-p49|Paleoproterozoic|Paleoproterozoic|Bryah Basin.|||Includes the Thaduna Formation.|Unconformably overlain by the Backdoor Formation.||
29869|Bryah Group|70826|6|Mentioned|p4, p6 tbl 2, p9|Paleoproterozoic|Paleoproterozoic|Bryah Basin.  Informally subdivided into upper and lower parts in Table 2, p6.|||Bryah Group, upper and Bryah Group, lower|||22-APR-20
29869|Bryah Group|71042|6|Mentioned|p66 fig 2, p96, p98||||||Includes the Horseshoe Formation.|||24-MAY-19
29869|Bryah Group|71269|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen, West Australian Craton. Of Bryah Basin. See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, glengarry_100k_geologyp_lut.csv, glengarry_500k_interpgeop_lut.csv.|2014-1920 Ma (inferred)||Includes Horseshoe Formation, Karalundi Formation, Narracoota Formation, Ravelstone Formation, Trillbar Formation.||Sandstone; minor shale and conglomerate|
29869|Bryah Group|71468|6|Mentioned|p25, p37|Orosirian|Orosirian|Geological province: Capricorn Orogen, Yilgarn Craton.|2030-1990 Ma|||||20-AUG-19
29869|Bryah Group|71484|5|Briefly described|p122-123,125-126,128-129,134,139|||Geological province:  Of Bryah Basin.|||Includes Horseshoe Formation, Ravelstone Formation, Narracoota Formation and Karalundi Formation.|Overlain unconformably by Padbury Group/Labouchere Formation.||30-AUG-19
29869|Bryah Group|72034|6|Mentioned|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Mentioned as parent unit. Age assumed from constituents. No other data. Informally divided into upper and lower parts, |||Includes in upper part: Horseshoe Formation, Ravelstone Formation; lower part: Karalundi Formation, Trillbar formation, Narracoota Formation.|||
29869|Bryah Group|73102|5|Briefly described|p3|||Yilgarn Craton.|||||Turbiditic sandstone and siltstone with minor iron-formation overlying intrusive and volcaniclastic metamafic and meta-ultramafic rock.|
29869|Bryah Group|73442|5|Briefly described|p3|||Yilgarn Craton.|||||Turbiditic sandstone and siltstone with minor iron-formation overlying intrusive and volcaniclastic metamafic and meta-ultramafic rock.|
30238|Bubble Well Member|7471|5|Briefly described|p8, Map legend|Proterozoic|Proterozoic|||Of the Juderina Formation.|||Chert breccia derived from stromatolitic carbonate rocks.|
30238|Bubble Well Member|12099|5|Briefly described|p675, 677, 679, 683,Fig.4, p681 Fig.6|Rhyacian|Rhyacian|Evaporitic rocks deposited in a sabkha-type environment. Deposition age given by Pb-Pb date on stromatolitic carbonates (Woodhead and Hergt, 1997).|2173 +/- 64 Ma.|Unit in Juderina Formation.||||04-MAR-13
30238|Bubble Well Member|22940|4|Described|Table 2 p12|||Of Juderina Formation, Yerrida Group.||||||15-DEC-08
30238|Bubble Well Member|23413|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Juderina Formation, Yerrida Basin||||||
30238|Bubble Well Member|23529|5|Briefly described|p7|Paleoproterozoic|Paleoproterozoic|Parent: Yerrida Group||||||07-NOV-08
30238|Bubble Well Member|23581|5|Briefly described|Map legend||Paleoproterozoic|Of the Juderina Formation in the Windplain Subgroup in the Yerrida Group in the Yerrida Basin||||||07-NOV-08
30238|Bubble Well Member|23586|4|Described|p17|Paleoproterozoic|Paleoproterozoic|Of Juderina Formation. Underlying unit Finlayson Member. Geological Province: Yerrida Basin.||||||07-NOV-08
30238|Bubble Well Member|23589|5|Briefly described|p6 Table 2|||2173+/-11 Ma (Pb-Pb isochron). Of Juderina Formation.||||||
30238|Bubble Well Member|23593|4|Described|p9|Paleoproterozoic|Paleoproterozoic|2258+/-180 Ma, 2173+/-64 Ma (Pb-Pb isochrons). Of Juderina Formation. Underlying unit Finlayson Member. Geological Province: Yerrida Basin.||||||07-NOV-08
30238|Bubble Well Member|23597|5|Briefly described|p9|||Of Juderina Formation. Geological Province: Yerrida Basin.||||||
30238|Bubble Well Member|23600|5|Briefly described|p8|Archean|Archean|Age: 2173+/-80 Ma (Pb-Pb isochron)[so who decided it was Archean???]. Of Juderina Formation. Underlying unit Finlayson Member. Geological Province: Yerrida Basin.||||||04-MAR-13
30238|Bubble Well Member|23611|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|See also page 33 Appendix 1. Of Windplain Subgroup. Geological Province: Yerrida Basin.||||||07-NOV-08
30238|Bubble Well Member|23744|5|Briefly described|p10 Table 1|Paleoproterozoic|Paleoproterozoic|See also page 11. Of Juderina Formation. Geological Province: Yerrida Basin.||||||07-NOV-08
30238|Bubble Well Member|23747|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|Age: 2173+/-64 Ma and 2258+/-180 Ma (Pb-Pb isochron). Of Juderina Formation. Geological Province: Yerrida Basin.||||||07-NOV-08
30238|Bubble Well Member|23749|5|Briefly described|p3 table 1|Proterozoic|Proterozoic|of Juderina Formation. Geological Province: Yerrida Basin.||||||
30238|Bubble Well Member|23759|4|Described|p17|Paleoproterozoic|Paleoproterozoic|Of Juderina Formation. Underlying unit Finlayson Member. Geological Province: Yerrida Basin.||||||07-NOV-08
30238|Bubble Well Member|23865|5|Briefly described|p171|Paleoproterozoic|Paleoproterozoic|Of Juderina Formation, Windplain Subgoup. Geological Province: Yerrida Basin. Age: 2173+/-64Ma (Pb-Pb isochron).||||||07-NOV-08
30238|Bubble Well Member|24021|3|Fully described|p12|Paleoproterozoic|Paleoproterozoic|Age: 2173 +/- 64Ma (Pb-Pb isochron). Parent: Juderina Formation. Geological Province: Yerrida Basin.||||||20-JAN-10
30238|Bubble Well Member|24022|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Juderina Formation. Geological Province: Yerrida Basin.||||||07-NOV-08
30238|Bubble Well Member|24028|5|Briefly described|p289|Paleoproterozoic|Paleoproterozoic|Of Juderina Formation.  Age: 2258+/-180Ma (Pb-Pb isochron).   Geological Province: Yerrina Basin.||||||07-NOV-08
30238|Bubble Well Member|43836|5|Briefly described|Map Legend||Proterozoic|of Juderina Formation.||||||
30238|Bubble Well Member|43843|5|Briefly described|Map Legend||Proterozoic|||||||
30238|Bubble Well Member|49893|4|Described|p11|Proterozoic|Proterozoic|Of the Juderina Formation (Yerrida Group). Geological Province: Yerrida Basin. Age: 2173+/-80 Ma (Pb-Pb isochron, Woodhead and Herst, 1997). Interfingers with the Finlayson Member. See also p3 Table 1.||||||
30238|Bubble Well Member|49912|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Juderina Formation (Yerrida Group).  Stromatolitic chert and chert breccia; minor dolomite.  Geological Province:  Yerrida Basin.||||||
30238|Bubble Well Member|50222|5|Briefly described|p320 Fig. 3, p321|Paleoproterozoic|Paleoproterozoic|Of the Juderina Formation (Windplain Group).  Stromatolitic carbonate and eavporitic rocks.  Age: 2.17Ga (Pb-Pb, Woodhead and Hergt, 1997).  Max. thickness: ~160m.   Geological Province: Yerrida Basin.  See also p322.||||||07-NOV-08
30238|Bubble Well Member|62289|4|Described|plate 1, p6, p7 Fig. 3-Fig. 4, p9-11|Palaeoproterozoic|Palaeoproterozoic|Of Juderina Formation, Windplain Subgroup, Yerrida Group; defined by Occhipinti et al. (1997); type locality given; stromatolitic chert, silicified evaporitic carbonate, chert breccia (replacing dolomite); pseudomorphs of evaporitic minerals (anhydrite, gypsum, halite and shortite); thickness: ~160 m; Age: Pb-Pb isochron 2173 +/- 64 Ma from stromatolitic carbonate rocks, depositional age.||||||
30238|Bubble Well Member|63866|5|Briefly described|p165|Rhyacian|Rhyacian|Yerrida Basin. An additional Pb-Pb isochron age of 2173 +/- 64 Ma is provided from Woodhead and Hergt, 1997. Both isochron ages are interpreted as the age of deposition.|2258 +/- 180 Ma (Russell et al., 1994)|Juderina Formation||||
30238|Bubble Well Member|64580|4|Described|map legend||Paleoproterozoic|Of Juderina Formation. Stromatolitic chert, silicified evaporitic carbonate, and chert breccia (replacing dolomite); pseudomorphs of evaporitic minerals (anhydrite, gypsum, halite and shortite).||||||15-DEC-08
30238|Bubble Well Member|65264|5|Briefly described|p27|||Of Juderina Formation. Geological province: Yerrida Basin. Comprises evaporites and laminated stromatolitic chert and carbonate beds.||||||07-FEB-11
30238|Bubble Well Member|65419|2|Defined|p6, p7, p8, pp10-18, p47.|Paleoproterozoic|Paleoproterozoic|Named after Bubble Well. Measured type section at 'Eagle Roost'. About 160 m thick. Age from Pb-Pb isochron from stromatolitic carbonate. Russell et al. (1994) derived an age of 2258 +/- 180 Ma by the same method. Evaporitic units, carbonates and chert breccia, previously assigned to the Finlayson Sandstone (Juderina Formation) by Gee and Grey (1993), are now included in this unit.|2173 +/- 64 Ma (Woodhead and Hergt, in press).|Unit in Juderina Formation.||Conformably overlies Finlayson Member. Is gradationally overlain by Johnson Cairn Formation. Is locally overlain unconformably by Yelma Formation (Earaheedy Group).|Chert breccia; shale; cyclic, biostromal, silicified evaporitic carbonate with stromatolites; laminated chert nodular anhydrite and gypsum rosettes (replaced by silica), halite; domal, conical and crested stromatolites.|
30238|Bubble Well Member|65472|5|Briefly described|p3 Fig.2|||Yerrida Basin. Age: from Fig.2, after Pirajno et al. 2004.|2.17 Ma Pb-Pb carbonate|Of Juderina Formation.||||24-SEP-15
30238|Bubble Well Member|65913|4|Described|p3 Table 1, pp5-6. |Paleoproterozoic|Paleoproterozoic|Not exposed in this map area. The two ages are Pb-Pb isochrons: (a) Russell et al. 1994; (b) Woodhead and Hergt 1997.|(a) 2258 +/- 180 Ma; (b) 2173 +/- 64 Ma.|Unit in Juderina Formation.|||Siltstone passing upwards into dolostone, with cherty microbial and stromatolitic beds overlain by a quartz arenite bed.|
30238|Bubble Well Member|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic|Yerrida Basin||Juderina Formation|||Stromatolitic chert, silicified evaporitic carbonate, and chert breccia (replacing dolomite); pseudomorphs of evaporitic minerals (anhydrite, gypsum, halite and shortite).|05-AUG-15
30238|Bubble Well Member|69003|4|Described|p10-12|||Yerrida Basin. Contains distinctive stromatolite taxa, eg Segosia finlaysoniensis, used in Basin-wide correlation.|c.2170 Ma (Pb-Pb).|Juderina Formation.||Conformably overlies Finlayson Member.|Includes stromatolitic carbonates.|
30238|Bubble Well Member|69152|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin [??]||Juderina Formation|||Stromatolitic chert, silicified evaporitic carbonate, and chert breccia (replacing dolomite); pseudomorphs of evaporitic minerals (anhydrite, gypsum, halite and shortite).|24-SEP-15
30238|Bubble Well Member|69596|5|Briefly described|p9-10, p37|||Yerrida Basin.|c.2170 Ma (Pb-Pb: Wodhead and Hergt, 1997).|Juderina Formation.|||Stromatolitic carbonates.|
30238|Bubble Well Member|70153|5|Briefly described|100k_geologyp10_lut.csv|Paleoproterozoic|Paleoproterozoic||c.1298 Ma (Inferred).|Juderina Formation|||Stromatolitic chert, silicified evaporitic carbonate, and chert breccia (replacing dolomite); pseudomorphs of evaporitic minerals (anhydrite, gypsum, halite and shortite).|
30238|Bubble Well Member|70804|5|Briefly described|p2|||New name.||Juderina Formation||||
30238|Bubble Well Member|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sedimentary breccia, chert, crystalline dolostone/dolomite|
30238|Bubble Well Member|71269|4|Described|1m_geologyp12_lut.csv|||Geological province: Capricorn Orogen, West Australian Craton. Of Yerrida Basin. Events: Capricorn Orogeny (1817-1772 Ma). See 1m_geologyp12_lut.csv, glengarry_100k_geologyp_lut.csv.||Unit of Juderina Formation.|||Sandstone, siltstone, claystone, basalt and tuff, arkose, conglomerate|
30238|Bubble Well Member|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen. Of Earaheedy Basin. See 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv, 100k_geologysub10_lut.csv.||Unit of Juderina Formation.|||Stromatolitic chert, silicified evaporitic carbonate, and chert breccia (replacing dolomite); pseudomorphs of evaporitic minerals (anhydrite, gypsum, halite and shortite)|
30238|Bubble Well Member|71484|4|Described|p122,124,126-127,133|Rhyacian|Rhyacian|Geological province: Of Yerrida Basin. Thickness: up to 100m thick. Records evaporitic and coastal carbonate depositiom. Biostratigraphic correlation of stromatolite taxa yield inferred age of 2200-2100 Ma, consistent with Pb-Pb model age of 2173+\-64 Ma (Woodhead and Hergt, 1997). Previously only mapped around southern part of the Yerrida Basin, but has since been intersected in drillholes at 1000m depth in the NE part of the basin.|c. 2200 Ma|Unit of Juderina Formation.||Overlain conformably to unconformably by Juderina Formaton. Underlain by Finlayson Member.|Stromatolitic carbonate, in places containing evaporitic beds.|30-AUG-19
25816|Budjan Creek Formation|23780|5|Briefly described|p129|Archean|Archean|Age: ~3308+/-5 Ma||||||07-NOV-08
25816|Budjan Creek Formation|24184|4|Described|p702, p699 Fig.3|Archean|Archean|Overlain by Gorge Creek Group. Underlain by  Wyman Formation. Geological Province: Pilbara Craton. Max Thickness: 1200m. Age: ca. 3308 Ma||||||07-NOV-08
25816|Budjan Creek Formation|24185|5|Briefly described|p734, p737 Tb.2|Archean|Archean|Age: ca. 3325-3308 Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
25816|Budjan Creek Formation|24531|5|Briefly described|p5 Tb. 1|Archean|Archean|Age: c.3308Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
25816|Budjan Creek Formation|24550|5|Briefly described|p31 Tb. 3.1|Archean|Archean|Conglomerate, sandstone, siltstone, felsic volcanics. Age: >3308Ma. Max. thickness: 1.2km.||||||07-FEB-11
25816|Budjan Creek Formation|31853|2|Defined|p62|Archean|Archean|||||||07-NOV-08
25816|Budjan Creek Formation|36874|6|Mentioned|p86|||||||||
25816|Budjan Creek Formation|39444|6|Mentioned|p11|||See also Table 1||||||
25816|Budjan Creek Formation|41252|6|Mentioned|p49|||||||||
25816|Budjan Creek Formation|45923|14|Not recorded|p.9|||U?Archeozoic.||||||
25816|Budjan Creek Formation|50381|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
25816|Budjan Creek Formation|50427|4|Described|p182 Fig.5|Archean|Archean|Age: 3310 Ma. Unconformably overlies Kelly Subgroup and Wyman Formation. Conformably overlain by Golden Cockatoo Formation, unconformably by Sulphur Springs Group. Of Pilbara Supergroup.||||||14-APR-11
25816|Budjan Creek Formation|50430|4|Described|p158 Tb.1||Archean|Local in extent. Deposited <3308 Ma. Clastic and felsic volcanic rocks. In East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
25816|Budjan Creek Formation|50544|6|Mentioned|p39|Archean|Archean|Age: c.3308Ma (Bagas and Van Kranendonk, in prep).  Not on the YARRIE sheet.||||||07-NOV-08
25816|Budjan Creek Formation|61253|5|Briefly described|p51|||Succession of clastic and felsic volcaniclastic rocks. Unconformably overlies the Kelly Group.  Geological Province: Pilbara Craton.||||||
25816|Budjan Creek Formation|63417|5|Briefly described|Map legend|Archean|Archean|Of the Sulphur Springs Group (Pilbara Supergroup). Age: <3228Ma. Geological Province: Pilbara Craton. Siliciclastic and felsic volcaniclastic rocks; local basalt; metamorphosed.||||||07-NOV-08
25816|Budjan Creek Formation|63441|3|Fully described|p4 Tb. 1, p21|Archean|Archean|Now placed at top of Sulphur Spr.Gp (Van K. 2006). Overlies Kelly Gp. Coarse-gr.siliciclastic rocks, felsic volcaniclastic sst, shale + local chert + minor dacitic tuff + pillowed basalt. Age 3308+/-5 -3228+/-6Ma. Max.thick:1200m.Geol.prov: Pilbara Craton||||||07-FEB-11
25816|Budjan Creek Formation|63538|4|Described|p6 Fig. 3|Archean|Archean|Of Sulphur Springs Group. Overlain by Pincunah Hill Formation. Geological Province: Pilbara Craton. Sedimentary rocks.||||||19-APR-13
25816|Budjan Creek Formation|64327|5|Briefly described|p61|Archean|Archean|Unconformably overlies the Warrawoona Group; unconformably overlain by Gorge Creek Group rocks. Age: c.3310Ma.||||||07-NOV-08
25816|Budjan Creek Formation|64328|4|Described|p54, p58|Archean|Archean|Formerly part of De Grey Group - reasons for revision presented in detail. Unconformably overlies Kelly + Salgash Subgroups (Warrawoona Gp); unconformably overlain by Gorge Creek Gp. Age: 3308+/-5Ma. Max. thickness: 1.5km. Detailed lithology is given||||||07-FEB-11
25816|Budjan Creek Formation|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Pilbara Supergroup. Geological Province: Pilbara Craton. Consists of dacitic tuff with quartz and feldspar phenocrysts as well as felsic volcaniclastic sandstone, shale, and local grey, white, and black chert, minor dacitic tuff; metamorphosed.||||||29-OCT-12
25816|Budjan Creek Formation|65008|4|Described|p5, p7, p8, p11, p12, p14, p15, p41|Paleoarchean||East Pilbara Granite-Greenstone Terrane. Geochronology by: D.R. Nelson, 2001, GSWA Record 2001/2, p. 129-132, 140-148, 175-177. Wrongly shown as part of Warrawoona Group in fig5, p8. May belong to the Sulphur Springs Group?|< ca. 3308 Ma|Of the Pilbara Supergroup||Underlain by the Warrawoona Group. Unconformably overlain by the Corboy Formation, Gorge Creek Group. Unconformably underlain by the Charteris Basalt? and Wyman Formation.|Comprises a succession of felsic volcaniclastic sandstone, shale, local chert, minor dacitic tuff, dacitic tuff with quartz and feldspar phenocrysts, and minor pillowed basalt.|29-MAR-16
25816|Budjan Creek Formation|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton. Mapped as three sub-units.|<3308 Ma (Blake 2001).|Of Pilbara Supergroup.|||Tholeiitic basalt, generally pillowed, minor massive komatiitic basalt, weakly metamorphosed; dacitic tuff with quartz and feldspar phenocrysts; felsic volcaniclastic sandstone, shale, and local grey, white and black chert, weakly metamorphosed.|
25816|Budjan Creek Formation|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Mapped as three sub-units.|<3328 Ma.|Of Sulphur Springs Group.|||Basalt, generally pillowed, minor komatiitic basalt, metamorphosed; tuffaceous volcaniclastic sandstone, dacitic composition, weakly metamorphosed; felsic volcaniclastic sandstone, shale, local grey, white and black chert, weakly metamorphosed.|
25816|Budjan Creek Formation|65827|3|Fully described|p6 Tb.1, p9 Fig.3, p12 Tb.3, p28-31|Paleoarchean|Paleoarchean|Of Sulphur Springs Group. Deposition <3228 Ma: detrital zircon (Van Kranendonk et al. 2004). Unconformably underlies Farrel Quartzite, Gorge Creek Group; unconformably overlies or faulted against Charteris Basalt. Over 1.3 km thick. A mixed succession of basalts, porphyritic dacitic tuff, felsic volcaniclastic sandstone and shale, local chert; minor dacitic tuff.||||||
25816|Budjan Creek Formation|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Sulphur Springs Group. Age shown as <3228 Ma. Siliciclastic and felsic volcaniclastic rocks; local basalt; metamorphosed.||||||
25816|Budjan Creek Formation|66745|4|Described|pp51-55, p57.|Mesoarchean|Mesoarchean|Numerous stacked progradational cycles were interpreted as evidence of intracratonic rifting progressing to deposition on a rifted continental margin. Age, sedimentology and tectonic setting support re-assignment from Sulphur Springs Group.|Maximum deposition age 3220 Ma.|Recently reassigned to Soanesville Group: removed from Sulphur Springs Group.||Unconformably overlies the Kelly Group.|A succession of clastic sedimentary rocks.|
25816|Budjan Creek Formation|67201|5|Briefly described|p12 Tb.1|||In Pilbara Craton, Budjan Creek Basin, rift-related successions.|< 3220 Ma|||||
25816|Budjan Creek Formation|68035|6|Mentioned|p289|||On SE side of  East Pilbara Terrane.?shallow-water clastic successions and thick volcanic piles, in passive margin settings.|?3201 - 3165 Ma|||||
25816|Budjan Creek Formation|68284|5|Briefly described|p7|Paleoarchean|Paleoarchean|Kelly greenstone belt, East Pilbara Terrane.|<3220 Ma.|||Overlies Sulphur Springs Group. Is overlain by Farrel Quartzite.||
25816|Budjan Creek Formation|69012|5|Briefly described|Map Legend|||Soanesville Basin.|< 3228 Ma|Of the Soanesville Group.|||Felsic volcanic breccia; felsic volcaniclastic sandstone, shale, local chert, minor dacitic tuffaceous rocks; wacke, minor conglomerate; conglomerate with interbedded sandstone, siltstone and shale; all metamorphosed.|29-APR-14
25816|Budjan Creek Formation|69167|4|Described|geologyp_lut.csv|Mesoarchean|Paleoarchean|||Soanesville Group|||Conglomerate, interbedded with sandstone, siltstone, and shale; metamorphosed. Wacke, siltstone and conglomerate; all metamorphosed. Felsic volcanic breccia and volcaniclastic sandstone, shale and chert. Basalt, generally pillowed; metamorphosed.|
25816|Budjan Creek Formation|69301|4|Described|p9 Tb.1, p13, p21 Fig.8|||Pilbara Craton. East Pilbara Terrane. Budjan Basin. Rift-related successions.|Max depositional 3220 Ma, U-Pb zircon Nelson 2001|||Unconformably overlies Sulphur Springs Group of Pilbara Supergroup (regional unconformity). Is overlain by Soanesville Group.|Sedimentary rocks.|
25816|Budjan Creek Formation|69566|6|Mentioned|p236|||East Pilbara Granite-Greenstone Terrane.|2940 Ma.|George Creek Group.||||
25816|Budjan Creek Formation|69590|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Paleoarchean|Geological province: Pilbara Craton. Of Soanesville Basin. Events: Mosquito Creek Orogeny; North Pilbara Orogeny; Prinsep Orogeny; East Pilbara Terrane Rifting Event. Sample GSWA 168908 (crystal-lithic tuff) yielded an interpreted igneous crystallisation age of 3308+\-5 Ma for the tuff (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3228-3185 Ma (inferred; isotopic)|Unit of Soanesville Group.|||Conglomerate, interbedded with sandstone, siltstone, and shale; metamorphosed; felsic volcaniclastic sandstone, shale; chert, minor dacitic tuffaceous rocks; metamorphosed; basalt, generally pillowed; minor komatiitic basalt; metamorphosed.|
25816|Budjan Creek Formation|70022|6|Mentioned|p115|||East Pilbara Terrane.||Soanesville Group.||||
25816|Budjan Creek Formation|70775|5|Briefly described|p12|||Budjan Creek Basin.||||||
25816|Budjan Creek Formation|70884|6|Mentioned|p135|Archean|Archean|Geological province: East Pilbara Terrane, Pilbara Craton.|<3.23 Ga|Unit of Soanesville Gtroup.||Unconformably overlies the Wyman Formation.||16-AUG-19
25816|Budjan Creek Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Paleoarchean|Soanesville Basin.|Max age 3228+/-12 Ma, min age ~3190 Ma.|Soanesville Group|||Siliciclastic and felsic volcaniclastic rocks; local basalt; metamorphosed.|
25816|Budjan Creek Formation|72251|5|Briefly described|p54|Mesoarchean|Mesoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Soanesville Group.||Lowermost unit of Soanesville Group. Overlain by Corboy Formation. Underlain unconformably by Cangaroo Caves Formation.||
25816|Budjan Creek Formation|72668|5|Briefly described|p4, p14|||East Pilbara Terrane.Includes detrital zircons dated at 3228 +/-6 Ma.||Gorge Creek Group|||Coarse siliciclastic rocks, felsic volcaniclastic sandstone, shale, local chert and minor dacitic tuff.|12-JAN-22
25816|Budjan Creek Formation|73598|6|Mentioned|p1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Soanesville Group.||Unconformably overlies Kangaroo Caves Formation. Is overlain by Corboy Formation.||
78636|Buldania Granodiorite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton. Emplacement age, U/Pb SHRIMP, from GA_OZCHRON.|2655+/-6 Ma, 2660+/-9 Ma||Includes 4 unnamed subunits.||Composite intrusion; predominantly seriate biotite-hornblende granodiorite; biotite-rich monzogranite; metagranitic rock; amphibole-rich metamonzogranitic rock.|05-AUG-15
78636|Buldania Granodiorite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Misnamed as Buldania Formation in GA_rocks.csv and GA_geochron.csv. Ages by Fletcher and McNaughton (2001).|2660 +/- 9 Ma and 2655 +/- 6 Ma (SHRIMP).||||Feldspar and quartz phyric microgranite; metamorphosed. Hornblende bearing granodiorite, biotite rich monzogranite, metagranitic rock, amphibole metamonzogranitic rock.|
78636|Buldania Granodiorite|70802|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton.|||||Composite intrusion; predominantly seriate biotite-hornblende granodiorite|
78636|Buldania Granodiorite|71270|4|Described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton.|||||Predominantly seriate biotite-hornblende granodiorite; also hbl-bearing granodiorite, locally with biotite; bt-rich monzogranite, metagranitic rock and amphibole-rich metamonzogranitic rock.|
33826|Buldya Group|50205|5|Briefly described|p60|Neoproterozoic|Neoproterozoic|Officer Basin. Sub-horizontal and unmetamorphosed sedimentary rocks. (Referred to as SS1 in p59 Fig.1).|||Includes the Steptoe, Kanpa, Hussar, Browne, Lefroy Formations and the Townsend Quartzite.|||
33826|Buldya Group|61732|5|Briefly described|p37, p58 Fig.22|Cryogenian|Cryogenian|Includes Browne, Wahlgu, Turkey Hill and Lupton Formations. Geological Province: southern Officer Basin.||||||07-FEB-11
33826|Buldya Group|62453|4|Described|p5 Fig. 3, 10|Cryogenian|Tonian|Geological Province: Officer Basin. Max Thickness: 4500m.||||||
33826|Buldya Group|62987|5|Briefly described|p30|Neoproterozoic|Neoproterozoic|Mixed carbonate-clastic-evaporite succession - Townsend Quartzite, Lefroy, Browne, Hussar, Kanpa and Steptoe Formations; and probably Ilma Formation and Mason Conglomerate also. Overlain by Wahlgu Fm. Age range: ca 830 to 700Ma. Geol.Prov:Officer Basin.||||||
33826|Buldya Group|63022|5|Briefly described|p1014|||Comprises Browne, Hussar and Kanpa Formations. Mixed carbonate-clastic and evaporite succession. Overlies Cornelia Sandstone.  Age: ca 830 to ca 700Ma. Geological Province: Officer Basin.||||||10-AUG-07
33826|Buldya Group|63864|5|Briefly described|Map Legend|||Geological Province: Officer Basin.||||||15-JUL-08
33826|Buldya Group|64103|5|Briefly described|p400, p404, p405|||Geological Province: Officer Basin. Is a mixed carbonate - evaporite succession.||||||07-FEB-11
33826|Buldya Group|64580|4|Described|map legend||Neoproterozoic|Sandstone, siltstone, shale, dolomite, limestone, evaporites (halite, gypsum, anhydrite) in subsurface and diapirs.||||||15-DEC-08
33826|Buldya Group|64772|5|Briefly described|p15|||Of Grey et al (2005). Geological province: Officer Basin. Lateral equivalent to Sunbeam Group.||||||07-FEB-11
33826|Buldya Group|65363|6|Mentioned|p5 Fig.4, p6 Fig.5. |Neoproterozoic|Neoproterozoic||||Includes Lefroy, Browne, Hussar, Kanpa and Steptoe Formations and Townsend Quartzite.|||
33826|Buldya Group|65365|5|Briefly described|p5, p8 Fig.3, p10|Cryogenian|Cryogenian|Western Officer Basin. Includes Browne, Hussar, Steptoe and Kanpa Formations and Keene Basalt.||||||19-MAR-12
33826|Buldya Group|65366|5|Briefly described|p19, 21, 22, 23 Fig. 3, p24|Cryogenian|Cryogenian|Western Officer Basin.|||Includes Kanpa, Hussar, Lefroy, Steptoe, Townsend and Browne Formations.|||19-MAR-12
33826|Buldya Group|65371|5|Briefly described|p54 Fig. 1|||Officer Basin. Unconformable on ?Cornelia Sandstone. Disconformably overlain by Wahlgu Formation. Includes Browne Formation, Hussar Formation, Kanpa Formation, ?Keene Basalt||||||
33826|Buldya Group|66427|6|Mentioned|p40 Fig.1|||NW Officer Basin.|||||Basal sand overlain by evaporitic mixed sequence.|
33826|Buldya Group|67244|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin.|||Includes Townsend Quartzite and Lefroy Formation.|||
33826|Buldya Group|67372|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin.|||||Undivided sedimentary rocks: sandstone, siltstone, shale, dolomite, limestone, evaporites (halite, gypsum, anhydrite) in subsurface and diapirs.|
33826|Buldya Group|67454|5|Briefly described|p563 Fig.2, p564, p569.|Neoproterozoic|Neoproterozoic|Officer Basin.|c.830 - c.720 Ma.||Includes Browne, Hussar and Kanpa Formations.|Is overlain disconformably by Wahlgu Formation.||
33826|Buldya Group|68270|5|Briefly described|p683,687|Cryogenian|Tonian|Western Officer Basin. |||Includes Kanpa Formation.|Overlain disconformably/unconformably by Pirrilyunka Formation.||
33826|Buldya Group|68995|6|Mentioned|p7 Fig.3|||Officer Basin. ||||||
33826|Buldya Group|69003|5|Briefly described|p4, p60-61|Neoproterozoic|Neoproterozoic|Officer Basin, Paterson Orogen.|||Townsend Quartzite; Lefroy, Browne, Hussar, Kanpa, Steptoe, Ilma Formations; Keene Basalt; Mason Conglomerate.|||
33826|Buldya Group|69091|5|Briefly described|p35, p43, p71 Fig.4.14|Neoproterozoic|Neoproterozoic|Western Officer Basin.|||Townsend Quartzite; Browne, Hussar, Kanpa and Steptoe Formations.|Is overlain by Pirrilyungka Formation.||26-SEP-14
33826|Buldya Group|69152|5|Briefly described|500k_geologyp08_lut||Neoproterozoic||||Includes Hussar, Kanpa and Steptoe Formations.|||
33826|Buldya Group|69153|5|Briefly described|GEOL_LUT_CSV files|Cryogenian|Neoproterozoic|Officer Basin, Centralian Superbasin|||||Sandstone, siltstone, shale, dolomite, limestone, evaporites (halite, gypsum, anhydrite) in subsurface and diapirs|
33826|Buldya Group|69438|6|Mentioned|p23:14|||Officer Basin.||||Lower part of this unit is correlated with Johnnys Creek beds (Amadeus Basin).||12-JUL-16
33826|Buldya Group|69606|6|Mentioned|p10|||Western Officer Basin. ||||Correlates with the Finke beds.||
33826|Buldya Group|69729|6|Mentioned|p82|||Officer Basin.||||||
33826|Buldya Group|69937|6|Mentioned|p8|||Officer Basin.||||Lower part correlated with Johnnys Creek Member (Bitter Springs Formation).||
33826|Buldya Group|70095|6|Mentioned|p17|||Officer Basin.||||Underlain by Cassidy Group/Bentley Supergroup/Warakurna Supersuite.||
33826|Buldya Group|70134|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Officer Basin.|||Townsend Quartzite.||Undivided sedimentary rocks: sandstone, siltstone, shale, dolomite, limestone, evaporites (halite, gypsum, anhydrite) in subsurface and diapirs (section only).|
33826|Buldya Group|70137|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin.|||Townsend Quartzite.|Is overlain by Lupton Formation.|Undivided sedimentary rocks: sandstone, siltstone, shale, dolomite, limestone, evaporites (halite, gypsum, anhydrite) in subsurface and diapirs.|
33826|Buldya Group|70416|5|Briefly described|p80|||Officer Basin. Contains the stromatolite Tungussia wilkatanna.||||||
33826|Buldya Group|70634|4|Described|100k_geologyp_lut,csv|Cryogenian|Neoproterozoic||635 Ma- 1000 Ma (Inferred)||Includes Lefroy Formation, Townsend Quartzite||Undivided sedimentary rocks; sandstone, siltstone, shale, dolomite, limestone, evaporites (halite, gypsum, anhydrite) in subsurface and diapirs|
33826|Buldya Group|70793|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Of Officer Basin (Phase 1), Centralian Superbasin. Events: Officer Basin Cenozoic diapirism (66-0.01 Ma); Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 500k_interpgeop_lut.csv, 2_5m_interpgeop15_lut.csv.|1000-720 Ma (inferred)||Includes Browne Formation, Hussar Formation, Kanpa Formation, Lefroy Formation, Steptoe Formation, Townsend Quartzite.||Undivided sedimentary rocks; sandstone, siltstone, shale, dolomite, limestone, evaporites (halite, gypsum, anhydrite) in subsurface and diapirs|
33826|Buldya Group|70802|6|Mentioned|500k_interpgeop14_lut.csv|||Of Officer Basin (Phase 1), Centralian Superbasin.||||||
33826|Buldya Group|70826|6|Mentioned|p5 tbl 2|||Supersequence 1, Centralian Superbasin.||||||20-APR-20
33826|Buldya Group|71211|6|Mentioned|p216|||Officer Basin. ||||||
33826|Buldya Group|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Townsend Quartzite|||sandstone, siltstone, shale, dolostone|
33826|Buldya Group|71268|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Of Officer Basin (Phase 1), Centralian Superbasin. Events: Officer Basin Cenozoic diapirism (66-0.01 Ma); Delamerian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|1000-720 Ma||Includes Browne Formation, Hussar Formation, Kanpa Formation, Lefroy Formation, Steptoe Formation,Townsend Quartzite.||Undivided sedimentary rocks; sandstone, siltstone, shale, dolomite, limestone, and evaporites (halite, gypsum, anhydrite) in subsurface and diapirs|
33826|Buldya Group|71270|5|Briefly described|GEOL_LUT_CSV files|||Of Officer Basin, Centralian Superbasin. See 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|||Includes Hussar Formation, Kanpa Formation, Steptoe Formation.|||
33826|Buldya Group|71288|6|Mentioned|p136|Neoproterozoic|Neoproterozoic|Paleomagnetic data from this unit locates Australia in low latitudes in the early Neoproterozoic.|830-720 Ma.|||||
33826|Buldya Group|72034|5|Briefly described|500k_interpgeop16_lut|Tonian|Tonian|Officer Basin (Phase 1).  Also listed as two informal subgroups: Buldya Group, lower (includes Townsend Quartzite, Lefroy Formation, and Browne Formation) and Buldya Group, upper (includes Hussar, Kanpa, and Steptoe Formations).||Sedimentary rocks, Centralian Superbasin Supersequence 1|Includes Ilma Formation.||Undivided sedimentary rocks; sandstone, siltstone, shale, dolomite, limestone, evaporites (halite, gypsum, anhydrite) in subsurface and diapirs.|
33826|Buldya Group|72094|6|Mentioned|p3 Fig 2, p4-5|Neoproterozoic|Neoproterozoic|Officer Basin.|||Includes Townsend Quartzite.|||
33826|Buldya Group|72369|5|Briefly described|p43|||Of Officer Basin. Lower part can be correlated with Johnnys Creek Formation, Bitter Springs Group (Amadeus Basin) (Grey et al 2011, Hill et al 2011).||||||
33826|Buldya Group|72375|5|Briefly described|p13|||Of Officer Basin.||||Correlable with Johnnys Creek Formation.||
33826|Buldya Group|73086|6|Mentioned|p39, p57|||Officer Basin.||||May partly correlate to Johnnys Creek Formation and Wallara Formation.||
33826|Buldya Group|73437|6|Mentioned|p151|Neoproterozoic|Neoproterozoic|Officer Basin.||||||
28411|Bulgadoo Shale|12733|6|Mentioned|p565.|Early Permian|Early Permian|Contains significant hydrocarbon source rocks.||Unit in Byro Group.||||
28411|Bulgadoo Shale|14228|6|Mentioned|p8, p18|Kungurian|Kungurian|||Byro Group||||05-OCT-16
28411|Bulgadoo Shale|23311|5|Briefly described|map legend|Artinskian|Artinskian|Of Byro Group.||||||
28411|Bulgadoo Shale|23312|5|Briefly described|map legend|Artinskian|Artinskian|Of Byro Group.||||||
28411|Bulgadoo Shale|23403|4|Described|p8|Early Permian|Early Permian|Of Byro Group.||||||
28411|Bulgadoo Shale|23726|5|Briefly described|p7 Fig 2b|Early Permian|Early Permian|Of Byro Group. Overlying unit Cundlego Formation. Underlying unit Mallens Sandstone. Geological Province: Carnarvon Basin.||||||
28411|Bulgadoo Shale|23815|4|Described|p284, 285|Artinskian|Artinskian|Geological Province: Merlinleigh Sub-basin. Of the Newman Subgroup. Overlying unit: Cundlego Formation (disconformable). Underlying unit: Mallens Greywacke (conformable). Max thickness: 520 m. Fossiliferous.||||||18-APR-05
28411|Bulgadoo Shale|24044|5|Briefly described|p541 Fig.2|Early Permian|Early Permian|Of Byro Group.||||||
28411|Bulgadoo Shale|30545|6|Mentioned|Fig.2|||Lower Permian||||||
28411|Bulgadoo Shale|31037|6|Mentioned|p1037|||Occurrence of Pseudoschistoceras.||||||
28411|Bulgadoo Shale|31251|6|Mentioned|p68|||Refers Thomas (1958) & McWhae et al. (1958)||||||
28411|Bulgadoo Shale|32648|6|Mentioned|p32|||Byro Gp.||||||
28411|Bulgadoo Shale|33701|6|Mentioned|Fig.1|||Artinskian.||||||
28411|Bulgadoo Shale|33710|6|Mentioned|Fig.1|||||||||
28411|Bulgadoo Shale|34287|6|Mentioned|p142|||L.- M.Permian||||||
28411|Bulgadoo Shale|34532|6|Mentioned|p225|||Byro Gp.||||||
28411|Bulgadoo Shale|36257|6|Mentioned|Table 2.1|||||||||
28411|Bulgadoo Shale|36387|6|Mentioned|p186|||||||||
28411|Bulgadoo Shale|36890|3|Fully described|p284|||Formerly Bulgadoo Series.||||||
28411|Bulgadoo Shale|37000|6|Mentioned|p23|||||||||
28411|Bulgadoo Shale|37294|6|Mentioned|p100|||||||||
28411|Bulgadoo Shale|37295|6|Mentioned|p54|||||||||
28411|Bulgadoo Shale|37304|6|Mentioned|p55|||||||||
28411|Bulgadoo Shale|37549|6|Mentioned|p110|||||||||
28411|Bulgadoo Shale|38493|6|Mentioned|p36|||||||||
28411|Bulgadoo Shale|39316|6|Mentioned|Fig.2|||||||||
28411|Bulgadoo Shale|40617|6|Mentioned|Fig.1|||||||||
28411|Bulgadoo Shale|41071|6|Mentioned|p34|||||||||
28411|Bulgadoo Shale|41271|3|Fully described|p95|||Formerly "Bulgadoo Series"||||||
28411|Bulgadoo Shale|41436|6|Mentioned|p42|||||||||
28411|Bulgadoo Shale|41438|6|Mentioned|Fig.11|||||||||
28411|Bulgadoo Shale|42116|5|Briefly described|Fig.1 P5|||||||||
28411|Bulgadoo Shale|42392|6|Mentioned|p116|||||||||
28411|Bulgadoo Shale|42540|6|Mentioned|p315|||||||||
28411|Bulgadoo Shale|42654|6|Mentioned|p4|||||||||
28411|Bulgadoo Shale|42994|6|Mentioned|p33|||||||||
28411|Bulgadoo Shale|43015|5|Briefly described|Table 1,p319|||||||||
28411|Bulgadoo Shale|43050|5|Briefly described|p7|||||||||
28411|Bulgadoo Shale|43255|5|Briefly described|map legend||Artinskian|of Byro Group.||||||
28411|Bulgadoo Shale|43256|5|Briefly described|19||Permian|||||||24-NOV-09
28411|Bulgadoo Shale|44219|14|Not recorded|p31||Artinskian|||||||
28411|Bulgadoo Shale|44344|14|Not recorded|p.11,12-13,24||Artinskian|Artinskian; part of Newman Subgroup of Byro Group. (G50-1). opp.4; map.||||||
28411|Bulgadoo Shale|44345|14|Not recorded|map legend||Artinskian|||||||
28411|Bulgadoo Shale|44532|4|Described|p.7,8,16, map|||Evaporite, salty. (G50-5).||||||
28411|Bulgadoo Shale|44533|5|Briefly described|map legend||Artinskian|Artinskian.||||||
28411|Bulgadoo Shale|44537|14|Not recorded|map legend||Artinskian|||||||
28411|Bulgadoo Shale|44657|14|Not recorded|p.9|||||||||
28411|Bulgadoo Shale|44994|6|Mentioned|Fig.7|||Correlation. Perm.||||||
28411|Bulgadoo Shale|45015|5|Briefly described|map legend|Artinskian|Artinskian|Of the Newman Sub-Group (Byro Group).||||||01-JUN-06
28411|Bulgadoo Shale|45016|2|Defined|p.137-143||Artinskian|Tb. at back, p.92,124,126,131,133,134,136,144,152,157,159-162. (F50-9,,13,G50-1,5).||||||
28411|Bulgadoo Shale|48610|14|Not recorded|Pl.1|||||||||
28411|Bulgadoo Shale|48831|14|Not recorded|p.37-39|||On many pages. p.24,34,37-39,41,43,59,69.||||||
28411|Bulgadoo Shale|48848|14|Not recorded|p.46,51,75,84,98|||||||||
28411|Bulgadoo Shale|49644|5|Briefly described|Table|||||||||
28411|Bulgadoo Shale|60331|5|Briefly described|p33 Fig.2|Kungurian|Kungurian|Of the Byro Group. Overlies Mallens Sandstone. Overlain by the Cundlego Formation. Geological Province: Southern Carnarvon Basin.||||||
28411|Bulgadoo Shale|61958|5|Briefly described|Map sheet 1|Artinskian|Artinskian|Of the Newman Sub-Group (Byro Group).||||||21-MAR-06
28411|Bulgadoo Shale|64580|5|Briefly described|map legend|||Of Middle Byro Group. Interbedded black mudstone, siltstone, and fine-grained sandstone.||||||15-DEC-08
28411|Bulgadoo Shale|64974|6|Mentioned|p147 Fig. 5|Kungurian|Kungurian|Geological Province: Carnarvon Basin.||||||24-JUN-09
28411|Bulgadoo Shale|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes brown siltstone.|
28411|Bulgadoo Shale|67200|5|Briefly described|p7 fig 5, p18 table 1|Kungurian|Artinskian|Thermal conductivity of 1.27 W/mK. See also p47, p54, app 2 p6. ||Byro Group||Overlies Mallens Sandstone, Overlain by Cundlego Formation|Crudely bedded siltstone/shale.|
28411|Bulgadoo Shale|69011|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin.||Of the Byro Group.||Overlain by the Cundlego Formation. Underlain by the Mallens Sandstone.|Comprises black pyritic shale and mudstone; minor sandstone interbeds.|
28411|Bulgadoo Shale|69028|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin. Mapped with Cundlego Formation, Quinnanie Shale and Wandagee Formation as a single unit.||Of the Byro Group.|||Interbedded black mudstone, siltstone and fine-grained sandstone.|06-MAY-14
28411|Bulgadoo Shale|69166|6|Mentioned|500k_geologyp08_lut.csv|Permian|Permian|||Byro Group||||
28411|Bulgadoo Shale|69182|6|Mentioned|Ch3 p55|||||||Overlain by the Cundlego Formation.||
28411|Bulgadoo Shale|69583|5|Briefly described|p130, Plate 3.|Permian|Permian|Southern Carnarvon Basin. Mapped as one unit with Cundlego Formation.||Byro Group.|||Black shale and siltstone overlain by fine-grained sandstone; hummocky and swaley cross-stratified.|
28411|Bulgadoo Shale|70795|4|Described|100k_geologyp_lut.csv|Kungurian|Kungurian|Also 100k_interpgeop_lut.csv|283-272 Ma|Byro Group|||Black pyritic shale and mudstone; minor sandstone interbeds.|
28411|Bulgadoo Shale|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||shale, siltstone, greywacke|
28411|Bulgadoo Shale|72910|4|Described|p10, p14, p18, p23, p33, p39, p41.|Kungurian|Kungurian|Thickness 60-270m. Type section: Minilya River, north of Wandagee Hill, 23d44m40sS; 114d30mE. Said to be Artinskian age p39.||Byro Group||Conformably overlies Mallens Sandstone. Conformably underlies Cundlego Formation.|Black pyritic shale, minor interbeds of fine sandstone.|
39508|Bullgarina Monzogranite|63417|5|Briefly described|Map legend|Archean|Archean|Of the Cleland Supersuite. Geological Province: Pilbara Craton. Biotite(-muscovite) monzogranite; medium- to coarse-grained, weakly metamorphosed.||||||07-NOV-08
39508|Bullgarina Monzogranite|63441|5|Briefly described|p9 Tb. 2|Archean|Archean|Of the Cleland Supersuite. Geological Province: Pilbara Craton.||||||07-FEB-11
39508|Bullgarina Monzogranite|65726|5|Briefly described|Map legend|Archean|Archean|||Of Mount Edgar Granitoid Complex.|||Biotite(-muscovite) monzogranite, medium- to coarse-grained.|
39508|Bullgarina Monzogranite|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. This unit was shown as part of the Mount Edgar Granitoid Complex in Version 1 of this map sheet (see Refid 65726).||Of Cleland Supersuite.|||Biotite(-muscovite) monzogranite, medium- to coarse-grained, weakly metamorphosed.|
39508|Bullgarina Monzogranite|65827|2|Defined|p6 Tb.2, p9 Fig 3, p26, p31, p57|Paleoarchean|Paleoarchean|New name. Small 1 x 4 km intrusion, 3 km NW of Bullgarina Hill. <3294 Ma. Intrudes Zulu Granodiorite; faulted/unclear contact with Bishop Creek Monzogranite. Of Cleland Supersuite; of Mount Edgar Granitic Complex. Mis-spelt as Bulgarina in Tb.2. Nonfoliated, medium- to coarse-grained, leucocratic biotite(-muscovite) monzogranite.||||||
39508|Bullgarina Monzogranite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Cleland Supersuite|||Biotite(--muscovite) monzogranite; medium to coarse grained; weakly metamorphosed.|
39508|Bullgarina Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3274-3224 Ma (inferred)|Unit of Cleland Supersuite.|||Biotite(-muscovite) monzogranite; medium to coarse grained; weakly metamorphosed|
39508|Bullgarina Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|||Cleland Supersuite|||Biotite(--muscovite) monzogranite; medium to coarse grained; weakly metamorphosed.|
26436|Bullo River Sandstone|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26436|Bullo River Sandstone|32660|5|Briefly described|Table 6|||||||||
26436|Bullo River Sandstone|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Reddish brown quartz sandstone, and conglomerate.||||||02-DEC-04
26436|Bullo River Sandstone|32701|4|Described|Table 1|||Adelaidean||||||
26436|Bullo River Sandstone|32728|6|Mentioned|p16|||||||||
26436|Bullo River Sandstone|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26436|Bullo River Sandstone|33377|5|Briefly described|Table 2|||||||||
26436|Bullo River Sandstone|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26436|Bullo River Sandstone|37462|4|Described|Table 4.VI|||See also Fig.4.13.||||||
26436|Bullo River Sandstone|45112|5|Briefly described|Table 3|||||||||
26436|Bullo River Sandstone|48938|2|Defined|p54|Proterozoic|Proterozoic|?Adelaidean||||||
26436|Bullo River Sandstone|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Wolfe Creek Basin. Of Duerdin Group. Includes Black Point Sandstone Member. Unconformably overlies Shoal Reach Formation. Unconformably overlain by Bucket Spring Member. Quartz sandstone, conglomerate.||||||23-JUL-04
26436|Bullo River Sandstone|60682|4|Described|p17|Neoproterozoic|Neoproterozoic|Of Duerdin Group. Unconformably overlies Shoal Reach Formation. Overlain by Bucket Spring Member. Max. Thickness: >320m. Geological Province: Wolfe Creek Basin.||||||
26436|Bullo River Sandstone|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic |Of Duerdin Group, Wolfe Creek Basin. Includes Black Point Sandstone Member. Quartz sandstone, conglomerate||||||
26436|Bullo River Sandstone|68733|5|Briefly described|p177 Fig.2, p183|Cryogenian|Cryogenian|Victoria Basin.||Basal unit of the Duerdin Group.|Includes Black Point Sandstone Member (basal subunit).|Unconformably overlies Shoal Reach Formation.||05-DEC-17
26436|Bullo River Sandstone|69437|6|Mentioned|p22:4-5|Cryogenian|Cryogenian|||||||12-JUL-16
26436|Bullo River Sandstone|69442|4|Described|p27:1-2, 3 Tb.27.1|||Wolfe Basin. Assigned to Duerdin Group by Dunster et al. (2000). Restricted to  620 km2 of inaccessible country in C and SW AUVERGNE map area. Over 320m thick. Depositional environment not determined; possibly fluvial.||Duerdin Group.|Black Point Sandstone Member.|Overlies Shoal Reach Formation (Auvergne Group) mostly dis/unconformably; gradational at one location.|Red-brown to maroon quartz sandstone, typically cross-bedded, poorly sorted; conglomerate.|12-JUL-16
26436|Bullo River Sandstone|69673|5|Briefly described|p190|Neoproterozoic|Neoproterozoic|300m thick.||Duerdin Group|Includes Black Point Sandstone Member||Quartzose sandstone.|
26436|Bullo River Sandstone|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin. ||Duerdin Group|Includes Black Point Sandstone Member||Quartz sandstone, conglomerate.|
26436|Bullo River Sandstone|71080|6|Mentioned|p25|||Of Victoria Basin. Higher stratigraphic level than Jasper Gorge Formation.|||Includes Black Point Sandstone Member.|||
26436|Bullo River Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone|
26436|Bullo River Sandstone|73083|6|Mentioned|p8|Neoproterozoic|Neoproterozoic||||||Includes red beds.|
73594|Bullock Hide Intrusion|63441|5|Briefly described|p10 Tb.2|Archean|Archean|Of Orpheus Supersuite. Geological province: Western Pilbara Superterrane/Pilbara Craton.||||||07-FEB-11
73594|Bullock Hide Intrusion|64174|5|Briefly described|Map legend|Archean|Archean|Of the Orpheus Supersuite. Geological province: Pilbara Craton. Gabbro, leucograbbro, serpentinised peridotite and dunite, pyroxenite and minor anorthosite; metamorphosed.||||||04-DEC-08
73594|Bullock Hide Intrusion|64580|4|Described|map legend||Mesoarchean|Of Orpheus Supersuite. Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed.||||||15-DEC-08
73594|Bullock Hide Intrusion|67201|4|Described|p16-17 Fig.9, p23|Archean|Archean|In northwestern Pilbara Craton, Sholl Terrane, West Pilbara Superterrane. A layered ultramafic-mafic intrusion S of Roebourne, assigned to Andover Intrusion, may be a faulted section of this unit.|c. 3120 Ma|Railway Supersuite|||Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed.|22-NOV-16
73594|Bullock Hide Intrusion|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Orpheus Supersuite.|||Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed|
73594|Bullock Hide Intrusion|70775|5|Briefly described|p15, p32, p34, p36-p37, p66|Mesoarchean|Mesoarchean|Sholl Terrane, Pilbara Craton. |3122 +/- 3 Ma (Wingate and Hickman, 2009b)|Railway Supersuite||Intrudes the Nallana Formation.|Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite and minor anorthosite; metamorphosed.|
73594|Bullock Hide Intrusion|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||gabbro, anorthosite, peridotite|
73594|Bullock Hide Intrusion|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||3122+/-3 Ma|Railway Supersuite|||Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed.|
31683|Bullock Hole Intrusion|43822|5|Briefly described|map legend|Archean|Archean|Layered mafic intrusions approx. 2925 Ma||||||07-NOV-08
75568|Bullsbrook Formation|24160|6|Mentioned|p94|Cretaceous|Cretaceous|Perth Basin.||||||
75568|Bullsbrook Formation|44144|4|Described|p504 Tb.4-21, p516-517|Early Cretaceous|Early Cretaceous|Type Section: Near Bullsbrook East: 31o39'53''S 116o02'40'E. 76m thick fluvial rocks; valley-fill deposits.||||Overlain disconformably by Osborne Formation. Correlates with Warnbro Group.|Varicoloured alternating poorly sorted sandstone and siltstone, in part conglomeratic.|
75568|Bullsbrook Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone, conglomerate, dolostone|
25709|Bundera Calcarenite|23311|5|Briefly described|map legend|Pleistocene|Pleistocene|||||||
25709|Bundera Calcarenite|23403|4|Described|p10|Quaternary|Quaternary|||||||24-NOV-09
25709|Bundera Calcarenite|23620|5|Briefly described|p4 Fig. 4|Quaternary|Quaternary|Shoreline, marine and coastal eolian deposits; includes coastal lake deposits: commonly calcareous gypsiferous||||||
25709|Bundera Calcarenite|23726|5|Briefly described|p91|Quaternary|Pliocene|Underlying unit Exmouth Sandstone. Geological Province: Carnarvon Basin.||||||
25709|Bundera Calcarenite|23815|6|Mentioned|p305|Pleistocene|Pleistocene|Geological Province: Carnarvon Basin.||||||
25709|Bundera Calcarenite|23976|5|Briefly described|Map Legend|Quaternary|Quaternary|||||||
25709|Bundera Calcarenite|23977|5|Briefly described|Map Legend|Quaternary|Quaternary|||||||
25709|Bundera Calcarenite|23978|5|Briefly described|Map Legend|Quaternary|Quaternary|||||||
25709|Bundera Calcarenite|30504|6|Mentioned|p33|||||||||
25709|Bundera Calcarenite|30821|6|Mentioned|p59|||Stratigraphic sequence||||||
25709|Bundera Calcarenite|33593|1|Redefined|p113|Quaternary|Quaternary|||||||
25709|Bundera Calcarenite|35105|6|Mentioned|Fig.70|||||||||
25709|Bundera Calcarenite|36257|6|Mentioned|Table 2.1|||||||||
25709|Bundera Calcarenite|36890|6|Mentioned|p305|||||||||
25709|Bundera Calcarenite|37016|6|Mentioned|Map legend|Holocene|Pleistocene|Pleistocene to Holocene.||||||
25709|Bundera Calcarenite|38954|6|Mentioned|Table 1|||||||||
25709|Bundera Calcarenite|39427|4|Described|Table 1|||||||||
25709|Bundera Calcarenite|41271|3|Fully described|p194|||||||||
25709|Bundera Calcarenite|42116|5|Briefly described|p71|||||||||
25709|Bundera Calcarenite|61155|5|Briefly described|p15|Holocene|Late Pliocene|Overlies the Exmouth Sandstone.  Geological Province: Carnarvon Basin /onshore.||||||
25709|Bundera Calcarenite|66125|5|Briefly described|p133 Fig.4|||Ningaloo Reef area; onshore. Occurs between the present-day lagoon and the Jurabi Scarp.|||Tantabiddi, Jurabi Members.||Lagoonal and reef facies underlie and crop out in the coastal zone of littoral and aeolian sandy deposits.|
25709|Bundera Calcarenite|67200|5|Briefly described|p8 fig 6, |Quaternary|Pliocene|||||Overlies Exmouth Sandstone|Planar cross bedded sandstone, limestone and pebbly sandstone with invertebrate macrofossils.|
25709|Bundera Calcarenite|69558|6|Mentioned|p99|||||||Is equivalent to the Tamala Limestone.||
25709|Bundera Calcarenite|70826|6|Mentioned|p7 tbl 4|Quaternary|Quaternary|Northern Carnarvon Basin.||||||
25709|Bundera Calcarenite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||marine and coastal sediment|
79520|Bungarra Igneous Complex|69583|5|Briefly described|Plate 2|Neoarchean|Neoarchean|Youanmi Terrane, Yilgarn Craton.|c.2720 Ma.||||Layered mafic and ultramafic intrusive rocks; metamorphosed.|
79520|Bungarra Igneous Complex|70153|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Mesoarchean||2820 - 2735 Ma (inferred).||||Layered mafic and ultramafic intrusive rocks; metamorphosed.|
79520|Bungarra Igneous Complex|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Mesoarchean|Youanmi Terrane.|||||Layered mafic and ultramafic intrusive rocks; metamorphosed.|
24791|Bungle Bungle Dolomite|22440|5|Briefly described|p4,5|Stenian|Stenian|Age 1200- 1000Ma.||||||02-AUG-06
24791|Bungle Bungle Dolomite|22496|6|Mentioned|p10||Neoproterozoic|Mapped as Eliot Range Dolomite in the Ruby Plains sheet area||||||
24791|Bungle Bungle Dolomite|22716|5|Briefly described|table4, p236|Calymmian|Calymmian|May be equivalent to part of the Birrindudu Group.||||||
24791|Bungle Bungle Dolomite|22754|5|Briefly described|p11 Tb. 3|Mesoproterozoic|Mesoproterozoic|Geological Province: Osmond Basin.||||||
24791|Bungle Bungle Dolomite|22764|4|Described|Table1,p7||Carpentarian|Probably conformable on Mount Parker Sandstone and unconformable beneath Wade Creek Sandstone.||||||01-FEB-10
24791|Bungle Bungle Dolomite|22899|6|Mentioned|86|||||||||
24791|Bungle Bungle Dolomite|23314|5|Briefly described|333|||||||||
24791|Bungle Bungle Dolomite|23621|6|Mentioned|p56 Appendix|||||||||
24791|Bungle Bungle Dolomite|23809|5|Briefly described|p47 Fig. 42|Proterozoic|Proterozoic|Geological Province: Osmond Basin.  Correlates with Limbunya Group, misspelt as Lumbunya in text, (Birrindudu Basin), Namerinni Group (Ashburton Province) and McArthur Group (McArtgur Basin).||||||
24791|Bungle Bungle Dolomite|24173|5|Briefly described|p24|Mesoproterozoic|Mesoproterozoic|Of the Osmond Range sequence. Previously included Eliot Range Dolomite||||||02-AUG-06
24791|Bungle Bungle Dolomite|24503|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Dolarenite, dololutite, and dolorudite, and chert breccia; commonly stromatolitic; minor dolomitic sandstone, siltstone and mudstone, and stromatolitic chert.   Geological Province: Osmond Basin.||||||
24791|Bungle Bungle Dolomite|28255|6|Mentioned|p11|||Age is probably Adelaidean but may be as old as Carpentarian. East Kimberley area (WA).||||||08-JUN-05
24791|Bungle Bungle Dolomite|29805|6|Mentioned|p9|||||||||
24791|Bungle Bungle Dolomite|29809|6|Mentioned|p418|||||||||
24791|Bungle Bungle Dolomite|29813|4|Described|Table 2|||||||||
24791|Bungle Bungle Dolomite|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24791|Bungle Bungle Dolomite|30895|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian and/or Adelaidean||||||
24791|Bungle Bungle Dolomite|31393|6|Mentioned|Pl.25|||||||||
24791|Bungle Bungle Dolomite|32172|6|Mentioned|p9|||Refers Dow and Gemuts(1969) & Sweet et al.(1971)||||||02-AUG-06
24791|Bungle Bungle Dolomite|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24791|Bungle Bungle Dolomite|32660|5|Briefly described|Table 6|||||||||
24791|Bungle Bungle Dolomite|32728|5|Briefly described|p42|||Mention p16.||||||02-AUG-06
24791|Bungle Bungle Dolomite|33374|6|Mentioned|p6|||Correlation||||||
24791|Bungle Bungle Dolomite|35120|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24791|Bungle Bungle Dolomite|35950|6|Mentioned|p311|||||||||
24791|Bungle Bungle Dolomite|36048|6|Mentioned|p380|||||||||
24791|Bungle Bungle Dolomite|36532|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24791|Bungle Bungle Dolomite|36551|6|Mentioned|p22|||||||||
24791|Bungle Bungle Dolomite|36885|4|Described|p177|||||||||
24791|Bungle Bungle Dolomite|36898|5|Briefly described|p186|||||||||
24791|Bungle Bungle Dolomite|37371|6|Mentioned|p367|||||||||
24791|Bungle Bungle Dolomite|37462|4|Described|Table 4.V|||||||||
24791|Bungle Bungle Dolomite|38243|6|Mentioned|Fig.2|||||||||
24791|Bungle Bungle Dolomite|38988|6|Mentioned|Fig.4|||||||||
24791|Bungle Bungle Dolomite|43631|6|Mentioned|p24|||||||||
24791|Bungle Bungle Dolomite|43855|5|Briefly described|Map Legend||Proterozoic|||||||
24791|Bungle Bungle Dolomite|44155|4|Described|p251-252|||Type area in Osmond Range area. At least 1000m thick. Contains stromatolites. Probable part correlative of Tawallah and McArthur Groups in McArthur Basin.||||Overlies Mount Parker Sandstone conformably. Is overlain unconformably by Wade Creek Sandstone. Equivalent to Talbot Well Formation.|Banded and brecciated cherts, silicified oolite, bouldery cherty ironstone, dolomite and dolomitic shale; several quartz sandstone beds up to 30m thick.|18-MAY-15
24791|Bungle Bungle Dolomite|44317|4|Described|Table 2||Carpentarian|||||||
24791|Bungle Bungle Dolomite|44318|14|Not recorded|map legend|||Adelaidean or Carpentarian.||||||
24791|Bungle Bungle Dolomite|44324|14|Not recorded|p.10||Neoproterozoic|Tb.2. (Upper Proterozoic).||||||
24791|Bungle Bungle Dolomite|44325|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic. Defn on Tech.File SE/52-6.||||||
24791|Bungle Bungle Dolomite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
24791|Bungle Bungle Dolomite|45047|2|Defined|p76|early Adelaidean|late Carpentarian|Early Adelaidean or Late Carpentarian.||||||
24791|Bungle Bungle Dolomite|45112|6|Mentioned|p17|||||||||
24791|Bungle Bungle Dolomite|45140|2|Defined|p12-14, p39-40, p42, p58-60, p74|||See also Appx.p32. Dow and Gemuts (1969). Mapped as Kearney Beds by Casey and Wells (1964). Named after Bungle Bungle outcamp on Turner station. Unnamed basin NW of Birrindudu Basin. Type section is in Osmond Range, Dixon Range sheet area. Forms low mounds. 300m thick. Silicified stromatolitic dolomite contains microfossils.||||Conformably overlies Mount Parker Sandstone. Is overlain unconformably by Wade Creek Sandstone. Probable equivalent to Talbot Well Formation (Birrindudu Group).|Mainly dolomite, dolomitic shale; banded chert, brecciated chert, silicified oolite, bouldery chert ironstone containing possible stromatolitic structures, minor lithic arenite; local micaceous greywacke, siltstone and shale.|
24791|Bungle Bungle Dolomite|46861|6|Mentioned|p9|||||||||
24791|Bungle Bungle Dolomite|46864|5|Briefly described|p40|||||||||
24791|Bungle Bungle Dolomite|48938|6|Mentioned|p76|||Equiv. Limbunya Group||||||
24791|Bungle Bungle Dolomite|50225|5|Briefly described|p406 Fig. 10, p407|Mesoproterozoic|Mesoproterozoic|Geological Province: Osmond Basin.||||||07-FEB-11
24791|Bungle Bungle Dolomite|61732|6|Mentioned|p26|||||||||07-FEB-11
24791|Bungle Bungle Dolomite|63866|5|Briefly described|p130, p132, p137|||Osmond Basin.||||Unconformably overlies the Kimberley Group.|Dolomite, stromatolitic chert, sandstone and siltstone.|
24791|Bungle Bungle Dolomite|64104|6|Mentioned|p63 Fig.1, p75|Neoproterozoic|Neoproterozoic|Says 'Subsequently named Eliot Range Formation' [?]. Osmond Basin. Part of Osmond Range succession. Likely source of clasts in Fargoo Formation. [This article changes the age of a number of units, including this one, without explanation. Error in Figure 10?]||||||19-MAY-15
24791|Bungle Bungle Dolomite|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Dolarenite, dololutite, and dolorudite and chert breccia; commonly stromatolitic; minor dolomitic sandstone, siltstone, mudstone, and stromatolitic chert.||||||09-DEC-08
24791|Bungle Bungle Dolomite|65074|6|Mentioned|p353|||Osmond Range succession in the Halls Creek Orogen.||||Correlated with Gardiner Sandstone.||
24791|Bungle Bungle Dolomite|68244|6|Mentioned|p668|||Erosion and remobilisation of carbonate leading to abundant carbonate framework clasts and high carbonate content of lower Duerdin Group glaciogenic units (Fargoo and Mountain Valley Fms; Corkeron 2008).||||||
24791|Bungle Bungle Dolomite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Osmond Basin|Depositional age: 867+/-2 Ma SHRIMP||Includes 3 unnamed members||Dolarenite, dololutite, and dolorudite and chert breccia; commonly stromatolitic; minor dolomitic sandstone, siltstone, mudstone, and stromatolitic chert; members also include quartz sandstone|30-JUL-15
24791|Bungle Bungle Dolomite|69165|4|Described|100k_interpgeop_lut.csv|Neoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv, GA_geochron.csv.|867 Ma||||Dolarenite, dololutite, dolorudite, chert breccia; commonly stromatolitic; minor dolomitic sandstone, siltstone, mudstone and stromatolitic chert. Thin to medium bedded, fine to medium grained quartz sandstone.|
24791|Bungle Bungle Dolomite|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Osmond Basin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|2500-1600 Ma (Inferred)||||Dolarenite, dololutite, and dolorudite and chert breccia; commonly stromatolitic; minor dolomitic sandstone, siltstone, mudstone, quartz sandstone and stromatolitic chert|
24791|Bungle Bungle Dolomite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv.|1797 Ma||||Dolarenite, dololutite, dolorudite, chert breccia; commonly stromatolitic, minor dolomuitic sandstone, siltstone, mudstone and chert. Thin to medium bedded fine to medium grained quartz sandstone.|
24791|Bungle Bungle Dolomite|70812|5|Briefly described|p30, p43|Neoproterozoic|Paleoproterozoic|Highly prospective in places for Pb-Zn.||||||
24791|Bungle Bungle Dolomite|71267|4|Described|GEOL_LUT_CSV files|Neoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Osmond basin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|1797-541 Ma (inferred)||||Dolarenite, dololutite, and dolorudite and chert breccia; commonly stromatolitic; minor dolomitic sandstone, quartz sandstone, siltstone, mudstone, and stromatolitic chert|
24791|Bungle Bungle Dolomite|72034|5|Briefly described|500k_interpgeop16_lut|Neoproterozoic|Paleoproterozoic|Osmond Basin.|||||Dolarenite, dololutite, and dolorudite and chert breccia; commonly stromatolitic; minor dolomitic sandstone, siltstone, mudstone, and stromatolitic chert.|
24791|Bungle Bungle Dolomite|73255|6|Mentioned|p534 Fig.2, p546, p548 Fig.12|Tonian|Tonian|Contains Collenia frequens stromatolite fossils.|ca 1128 Ma|Osmond Range Succession||Overlies the Mount Parker Sandstone, underlies the Wade Sandstone.||
26440|Bunjinah Formation|23045|6|Mentioned|291 fig 8|||Parent Fortescue Group.||||||09-DEC-08
26440|Bunjinah Formation|23570|4|Described|p115|||See also p232 App. 1.  Supersedes the Bunjinah Pillow Lava Member of de la Hunty (1965).   Overlain by Jeerinah Fm; underlain by Pyradie Fm.   Max. thickness 900m.   Geol. Prov: Pilbara Craton||||||
26440|Bunjinah Formation|23575|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Underlying unit Pyradie Formation. Geological Province Hamersley Basin.||||||07-NOV-08
26440|Bunjinah Formation|23870|5|Briefly described|p224|||See also Bunjinah formation.  Of Fortescue Group.  Overlain by Jeerinah Formation.||||||
26440|Bunjinah Formation|24544|4|Described|p57 Fig.43|Archean|Archean|Of Fortescue Group. Overlies Pyradie Formation. Overlain by Jeerinah Formation. Basalt. Geological Province: Hamersley Basin.||||||07-NOV-08
26440|Bunjinah Formation|42471|5|Briefly described|p6, p4|||Equivalent to Bunjinah Pillow Lava Member of Mount Jope Volcanics (1965, 1968).||||||
26440|Bunjinah Formation|42472|5|Briefly described|Map legend|Archean||||||||07-NOV-08
26440|Bunjinah Formation|42686|5|Briefly described|map legend|Archean||||||||07-NOV-08
26440|Bunjinah Formation|42744|4|Described|p4|||||||||
26440|Bunjinah Formation|43119|4|Described|p7|||Of Fortescue Group.||||||09-DEC-08
26440|Bunjinah Formation|43262|5|Briefly described|Map Legend||Archean|Of Fortescue Group.||||||09-DEC-08
26440|Bunjinah Formation|43290|4|Described|p5||Archean|Of Fortescue Group.||||||09-DEC-08
26440|Bunjinah Formation|60706|5|Briefly described|p625 Fig.3|Archean|Archean|Of the Fortescue Group. Geological Province: Hamersley Basin.||||||07-NOV-08
26440|Bunjinah Formation|62129|3|Fully described|p6, p7-8|Archaean|Archaean|Of Fortescue Group. Conformably underlain by Pyradie Formation, conformably overlain by Jeerinah Formation. Thickness: 900m. Geological Province: Hamersley Basin. See p7-8 for more information.||||||17-DEC-12
26440|Bunjinah Formation|62130|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Geological Province: Hamersley Basin, Pilbara Craton. Pillowed and massive metabasaltic flows, metabasaltic breccia, metamorphosed volcanic sandstone, and minor chert.||||||23-MAR-09
26440|Bunjinah Formation|63367|5|Briefly described|p231 Fig.1.|Neoarchean|Neoarchean|||Unit in Fortescue Group.||Equivalent to Maddina Formation.||
26440|Bunjinah Formation|64384|5|Briefly described|p29 Tb. 5|Archean|Archean|Of the Fortescue Group. Geological province: southern Hamersley Basin.||||||07-FEB-11
26440|Bunjinah Formation|64580|4|Described|map legend||Neoarchean|Of Fortescue Group. Pillowed and massive basaltic flows; basaltic breccia; and basaltic volcanic sandstone; minor chert; amygdaloidal basalt flows occur in upper parts of formation; metamorphosed.||||||09-DEC-08
26440|Bunjinah Formation|64724|4|Described|p43, p42 Fig. 3|Neoarchean|Neoarchean|Basalt erupted during extension of the Hamersley Basin.||Of Fortescue Group.||||02-APR-12
26440|Bunjinah Formation|66217|5|Briefly described|p45.|||Fortescue Basin.||Unit in Fortescue Group.|||Subaqueous basaltic to komatiitic lavas and volcaniclastic rocks.|
26440|Bunjinah Formation|67025|5|Briefly described|p322 Table 3, pp324-325.|Archean|Archean|Hamersley Basin. Mean bulk susceptibility of this and other units is discussed in this article.||Unit in Fortescue Group.||||
26440|Bunjinah Formation|67201|4|Described|p28-30|||In northern Pilbara Craton, Fortescue Basin, South Pilbara Sub-basin.||Fortescue Group|||Dominated by tholeiitic basalts, with massive flows, associated with pillow lava and hyaloclastite breccia. Strongly amygdaloidal flows in upper part.|
26440|Bunjinah Formation|69028|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.||Of the Fortescue Group.|||Pillowed and massive basaltic flows; basaltic breccia and basaltic volcanic sandstone; minor chert; amygdaloidal basalt flows occur in upper parts of Formation; metamorphosed.|06-MAY-14
26440|Bunjinah Formation|69080|5|Briefly described|p687, p693|Neoarchean|Neoarchean|||Unit in Fortescue Group.||Overlies Pyradie Formation. Is overlain by Jeerinah Formation.||
26440|Bunjinah Formation|69166|5|Briefly described|500k_geologyp08_lut.csv|Neoarchean|Neoarchean|||Fortescue Group|||Pillowed and massive basaltic flows; basaltic breccia; and basaltic volcanic sandstone; minor chert; amygdaloidal basalt flows occur in upper parts of formation; metamorphosed.|
26440|Bunjinah Formation|69185|4|Described|GEOL_LUT_CSV files||Neoarchean|Geological Province: Pilbara Craton. Of South Pilbara Sub-basin, Hamersley Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 2717 Ma|Unit of Fortescue Group.|||Quartzofeldspathic conglomerate and sandstone; mudstone; and siltstone; metamorphosed; pillowed and massive basaltic flows; basaltic breccia; and basaltic volcanic sandstone; minor chert; amygdaloidal basalt flows occur in upper parts of formation.|
26440|Bunjinah Formation|69301|5|Briefly described|p17 Fig.6, p18 Fig.7|||Pilbara Craton. Fortescue Basin. South Pilbara Sub-basin, Sequence 3.||Fortescue Group||||
26440|Bunjinah Formation|69792|6|Mentioned|p1096 Fig.1|||Appears to be shown as equivalent to Maddina Formation.||Unit in Fortescue Group.||||22-JUN-20
26440|Bunjinah Formation|70795|6|Mentioned|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean|Also 500k_interpgeop14_lut.csv|2735-2629 Ma|||||
26440|Bunjinah Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||basalt, ash tuff, chert|
26440|Bunjinah Formation|71803|4|Described|p365-p369, p371, p374-p380, p385|Neoarchean|Neoarchean|Pilbara Craton. Geochemsitry discussed. An additional age of 2715 +/- 2 is also derived from Blake et al, 2004.|2718 +/- 3n Ma (Blake et al, 2004)|Fortescue Group||Lateral equivalent to the Maddina Formation.|Mafic lavas including subaerial and subaqueous (dominant) sheet flows with dacitic and rhyolitic volcaniclastic rocks.|
26440|Bunjinah Formation|71808|6|Mentioned|p8-p9, p117|||Hamersley Basin.||||Equivalent to the Maddina Formation.|Basalt.|
26440|Bunjinah Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|South Pilbara Sub-basin, Fortescue Basin.||Fortescue Group, sequence 4|||Pillowed and massive basaltic flows; basaltic breccia and basaltic volcanic sandstone; minor chert; amygdaloidal basalt flows occur in upper parts of formation; metamorphosed.|
26440|Bunjinah Formation|72712|5|Briefly described|p8, p9 Fig.5, p10 Fig.6.|Neoarchean|Neoarchean|Formation is c. 900 m thick in Hardey Syncline.|min age c. 2715 Ma.|Fortescue Group||Overlies Pyradie Formation and underlies Jeerinah Formation and is equivalent to Maddina Formation.|Includes massive submarine basalt and pillow basalt with minor hyaloclastite breccia and mafic volcaniclastic rock with upper parts characterized by highly vesicular basalt interbedded with hyaloclastite breccia.|
26440|Bunjinah Formation|73538|6|Mentioned|p4|Neoarchean|Neoarchean|Written as Maddina Formation / Bunjinah Formation. Ages of 2715 +/- 2 Ma and 2718 +/- 3 Ma were reported by Mole et al. (2018) for these units.|2715 +/- 2 Ma, 2718 +/- 3 Ma|Fortescue Group||Underlain by Pyradie Formation / Tumbiana Formation. Overlain by Jeerinah formation.|Mafic volcanics.|
78355|Bunnawarra Suite|69583|5|Briefly described|p49|Mesoarchean|Mesoarchean|Murchison Domain.||Windine Supersuite|Wurarga Granodiorite, Kynea Tonalite, Dromedary Bore Tonalite.|||
78355|Bunnawarra Suite|69584|6|Mentioned|p5 Fig.2|Mesoarchean|Mesoarchean||c. 2950 -2925 Ma|Windine Supersuite|Wurarga Granodiorite, Kynea Tonalite, Dromedary Bore Tonalite|||
78355|Bunnawarra Suite|69586|5|Briefly described|p22|Mesoarchean|Mesoarchean|Murchison Domain.||Windine Supersuite.|Wurarga Granodiorite; Kynea, Dromedary Bore Tonalites.|||
78355|Bunnawarra Suite|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton.|c.2950 Ma.|Thundellara Supersuite.|Kynea Tonalite.|||
78355|Bunnawarra Suite|70770|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c.2945 Ma.|Thundelarra Supersuite.|Dromedary Bore Granite.|||
78355|Bunnawarra Suite|70796|5|Briefly described|2_5m_interpgeop15_lut.csv|Mesoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. Affected by the Yilgarn Craton granite magmatism (3010  2600 Ma); Youanmi Terrane events (3131  2600 Ma). See also 100k_geologyl_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 155879.1.pdf, 198213.1.pdf, 203702.1.pdf, 203703.1.pdf, 203704.1.pdf, 211102.1.pdf, Badja100_2240_stratig.pdf, Bungar100_2539_stratig.pdf.|29642945 Ma|Thundelarra Supersuite|Includes the Dromedary Bore Granite and the Kynea Tonalite.|Coeval with the Gossan Hill Formation.||
78355|Bunnawarra Suite|70830|5|Briefly described|p9|||Murchison Domain.||Thundelarra Supersuite||||
78355|Bunnawarra Suite|71269|4|Described|GEOL_LUT_CSV files + geochron files|||Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Sample GSWA 155879 (granodiorite gneiss) yielded concordia intercept age of 2956+\-58 Ma, considered as a best estimate og the crystallsiation age of the igneous protolith.See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv.||Unit of Thundelarra Supersuite.|Includes Dromedary Bore Granite, Kynea Tonalite.|In contact with Norie Group.|Metatonalite and metagranodiorite as large, deformed rafts.|
78355|Bunnawarra Suite|72034|6|Mentioned|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Dromedary Bore Granite.|||
74871|Burnakura Tonalite|64891|5|Briefly described|p37 Fig. 2, p50-51 Tb. 1|Archean|Archean|Of Cullculli Suite (Annean Supersuite). Age: ?2750Ma. Geological province: Murchison Domain. Tonalite; metamorphosed.||||||07-FEB-11
78652|Burnside Granite (WA)|65487|5|Briefly described|p52, p56 Fig. 27, p59|Mesoproterozoic|Mesoproterozoic|1190-1170 Ma intrusion age. Intruded into the Nornalup Zone late in Stage II of the Albany-Fraser Orogeny. A voluminous porphyritic granite.||||||09-JAN-15
27729|Burra Monzogranite|9168|5|Briefly described|Map legend|Archaean|Archaean||||||Coarse porphyritic monzogranite|
27729|Burra Monzogranite|41914|4|Described|p19|||||||||
27729|Burra Monzogranite|42698|5|Briefly described|map legend|||||||||
27729|Burra Monzogranite|42892|4|Described|p39|||||||||
27729|Burra Monzogranite|60076|5|Briefly described|p45 App. 1|||[Agmbr]   Coarse-grained, biotite bearing, K-feldspar megacrysts.||||||
27729|Burra Monzogranite|65264|5|Briefly described|p46 Appdx. 1|Archean|Archean|Coarse-grained biotite monzogranite; K-feldspar megacrysts; generally homogeneous, deformed at margins; possible a composite intrusion.||||||07-FEB-11
27729|Burra Monzogranite|68066|5|Briefly described|p5 Fig. 2, p18, p20, p22, p23-30, map|Archean|Archean|Compositionally indistinguishable from Woolgangie Monzogranite. The Burra Monzogranite is so voluminous that it is probably not a simple monolithic unit; rather, it may comprise many separate and probably sheet-like intrusions, which have been folded.|||||Coarse porphyritic monzogranite; prominent megascopic microcline phenocrysts.|
27729|Burra Monzogranite|68655|5|Briefly described|GEOCHRON 142803.1|Neoarchean|Neoarchean|This age of igneous crystallisation is the preferred interpretation, with another zircon group aged 2676 +/- 19 Ma considered to be derived from the pegmatite dykes/veins.|2707 +/- 6 Ma (SHRIMP U-Pb zircon; Nelson, 1997).||||Medium-grained (2-3mm), equigranular biotite-muscovite granite containing subhedral platy biotite within an anhedral-granular matrix of quartz, sodic plagioclase and microcline feldspar. Numerous small pegmatite veins.|20-NOV-15
27729|Burra Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Coarse-grained biotite monzogranite; K-feldspar megacrysts; generally homogeneous, deformed at margins; possibly composite intrusion.|05-AUG-15
27729|Burra Monzogranite|69559|5|Briefly described|142803.1.pdf||Neoarchean|Geochronology dataset 411. Group 1: 2707+/-6 Ma. Group 2: 2676+/-19 Ma. The preferred interpretation is that Group 1 analyses provide the time of igneous crystallization of the monzogranite, whereas Group 2 analyses are of zircons derived from the pegmatite dykes|||||Weakly foliated monzogranite.|
27729|Burra Monzogranite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2687 +/- 6 Ma (isotopic).||||Coarse-grained biotite monzogranite; K-feldspar megacrysts; generally homogeneous, deformed at margins; possibly composite intrusion.|
27729|Burra Monzogranite|70156|5|Briefly described|142803.1.pdf|||Sample GSWA 142803 (biotite-muscovite granite) yielded an interpreted igneous crytallisation age of 2676+\-9 Ma (mean 207Pb/206Pb).|2676+\-9 Ma|||||
27729|Burra Monzogranite|70794|6|Mentioned|142803.1.pdf|||The preferred interpretation is that Group 1 analyses provide the time of igneous crystallization of the monzogranite, whereas Group 2 analyses are of zircons derived from the pegmatite dykes. Group 1: 2707+/-6 Ma, Group 2: 2676+/-19 Ma U/Pb SHRIMP (1996)||||||
27729|Burra Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv.|2687+\-6 Ma||||Coarse-grained biotite monzogranite; K-feldspar megacrysts; generally homogeneous, deformed at margins; possibly composite intrusion|
23446|Burragenup Member|40314|4|Described|Table 1|||||||||
23446|Burragenup Member|40367|2|Defined|p80|Holocene|Holocene|Of Safety Bay Sand. Overlain by Rosamel Member (erosional contact). Max. thickness: 40m. Unit of aeolian sand and soil sheets. Partly indurated along laminae casuing some lithification; abundant rhizocincretions.||||||24-MAR-14
23446|Burragenup Member|69788|4|Described|p1027, p1029-1030, p1032-1036|Holocene|Holocene|Of Semeniuk (1983). Outcrops as mounds up to 5m high.|8150 +/- 270 years BP (C-14), Mory (1995).|Basal unit in Safety Bay Sand.||Overlies Pinnacles Desert Member and Cooloongup Sand. Is overlain by Vittoria Member.|Light yellow, poorly cemented, cross-bedded to planar laminated, calcareous sand; contains numerous rhizoliths, commonly free-standing.|
23446|Burragenup Member|69840|5|Briefly described|p188, p186 Fig.3, p196 Fig.13, p197|Holocene|Holocene|Dating using Carbon-14 geochronology (Mory 1995).|0.00815 +/- 0.00027 Ma|Safety Bay Sand||Overlies Cooloongup Sand. Partially overlies Nambung Member.|Calcareous sand. c. 30% aragonite, remaining calcite.|
77941|Burrell Well Basalt|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2720 - 2680 Ma (inferred).|Two Sisters Subgroup|||Komatiitic basalt; locally pillowed; metamorphosed.|
77941|Burrell Well Basalt|70326|3|Fully described|p336,338,341-2,349,351,353-4,360,362-4|Neoarchean|Neoarchean|Geological province: Agnew region, Ora Banda Domain, Kalgoorlie Terrane, Yilgarn Craton. [Also referred to as Burrell Basalt on p342]. Subaqueous basalts that are compositionally gradational from the underlying Agnew Komatiite and become progressively more fractionated through time, starting in the komatiitic basalt field on the Jensen plot and finishing in the high-Mg tholeiite field. Contemporaneous to, and interdigitates with Redeemer Basalt. Thickness: 200m. Occurs sporadically on western limb Agnew Anticline, common in the Mount White Syncline. Major and trace element geochemical analysis on Table 4 p342-346.||||Interdigitates with Redeemer Basalt. Underlain by Agnew Komatiite. Correlable to Big Dick Basalt and Gleesons Basalt and Tripod Hill Komatiite.|Fine-grained basic (massive and pillow basalts). Texturally indistinguishable from Redeemer Basalt. Submarine pillow and sheet flows.|29-JUL-19
77941|Burrell Well Basalt|71212|5|Briefly described|intro p2|||Yilgarn Craton. ||Two Sisters Subgroup||||
77941|Burrell Well Basalt|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2711-2687 Ma (inferred)|Unit of Two Sisters Subgroup.|||Komatiitic basalt; locally pillowed; metamorphosed|
77941|Burrell Well Basalt|73151|5|Briefly described|p3, p5, p10, p12-13, p16|Neoarchean|Neoarchean|Yilgarn Craton. Kalgoorlie Terrane, Agnew Greenstone Belt.||Kalgoorlie Group||Overlies Agnew Komatiite, underlies Redeemer Basalt.|Pillow basalt.|
77941|Burrell Well Basalt|73596|6|Mentioned|p1152, 1156-1158, 1160, 1163, 1167|Neoarchean|Neoarchean|Agnew-Wiluna Greenstone Belt. Deep-water mafic-ultramafic lava fields and feeder intrusions.||Two Sisters Subgroup.||Overlies Agnew Komatiite. Is overlain by Redeemer, White Hope Basalts.||
77546|Burtville Granite|66880|5|Briefly described|p29. |Archean|Archean|Burtville Terrane, east Yilgarn Craton.|2716 +/- 3 Ma (Dunphy et al. 2003).||||HFSE-granitoid intruded into mafic-volcanic and sedimentary rocks.|01-NOV-12
78512|Burtville granodiorite|68107|5|Briefly described|p608 Fig.4, p617.|Neoarchean|Neoarchean|Laverton Greenstone Belt, Burtville Terrane.|2716 +/- 4 Ma (Dunphy et al. 2003).|||Intrudes the Burtville Sandstone.||
78512|Burtville granodiorite|71168|6|Mentioned|p10|Neoarchean|Neoarchean|Burtville Terrane, Yilgarn Craton.|c. 2716 Ma|||||
78512|Burtville granodiorite|73596|6|Mentioned|p1170|Neoarchean|Neoarchean|Laverton Greenstone Belt, Burtville Terrane. Appears as (formalised) Burtville Granodiorite.|2716 +/- 4 Ma.|||||
34924|Butcher Bird Monzogranite|22902|5|Briefly described|68|||Geol province Southern Cross Province||||||
34924|Butcher Bird Monzogranite|23531|5|Briefly described|p14.|||||||||
34924|Butcher Bird Monzogranite|23787|5|Briefly described|p11|Archean|Archean|Intrudes the Marda Complex.  Age: 2730+/-4Ma.  Geological Province: Yilgarn Craton.  See also p47.||||||07-NOV-08
34924|Butcher Bird Monzogranite|24167|4|Described|p27, p7 Fig.3, p31 Fig 20|||Age: 2730+/-4Ma (SHRIMP U-Pb, Nelson, 2001). Intruded by Chatarie Well Granite.  Intrudes Marda Complex. Geological Province: Yilgarn Craton.||||||
34924|Butcher Bird Monzogranite|24245|5|Briefly described|p7 Tb. 1|Archean|Archean|Granitoid intrusion.  Age: c.2.73Ga.  Geological Province: Yilgarn Craton.||||||07-NOV-08
34924|Butcher Bird Monzogranite|24335|5|Briefly described|Map legend|Archean|Archean|Age: c.2730Ma.  Geological Province: Yilgarn Craton||||||07-NOV-08
34924|Butcher Bird Monzogranite|24445|4|Described|p1, 12|Archean|Archean|Age: 2730 +/- 4Ma (SHRIMP U-Pb). Geological Province: Yilgarn Craton||||||07-NOV-08
34924|Butcher Bird Monzogranite|24446|5|Briefly described|Map legend|Archean|Archean|Fine- to medium-grained monxogranite; typically granophytic.  Age: c.2730Ma.   Geological Province: Yilgarn Craton.||||||07-NOV-08
34924|Butcher Bird Monzogranite|63778|5|Briefly described|p1125 Fig. 1, p1126 Tb. 1, p1127, p1129|Archaean|Archaean|Age: 2730+/-4Ma (U-Pb zircon). Intrudes the Marda Complex. Geological Province: Yilgarn Craton. More detailed information throughout the text.||||||18-MAR-09
34924|Butcher Bird Monzogranite|65265|6|Mentioned|p75|||High-level intrusive equivalent of the Marda Complex; has correspondingly been included in the formal stratigraphy of the Complex.||||||
34924|Butcher Bird Monzogranite|68108|6|Mentioned|p652|Neoarchean|Neoarchean|Coeval and possibly comagmatic with Marda Complex.|2730 +/- 4 Ma (Nelson 2001).|||||
34924|Butcher Bird Monzogranite|69152|4|Described|1m_geologyp08_lut.csv|Archean|Archean||||||Granophyric monzogranite; high-HFSE granite.|05-AUG-15
34924|Butcher Bird Monzogranite|70153|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean||2730 +/- 4 Ma (isotopic).|Marda Complex.|||Fine- to medium-grained monzogranite; typically granophyric; metamorphosed.|
34924|Butcher Bird Monzogranite|70156|4|Described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Of Marda Complex. Events: Youanmi Terrane events (3200-2600 Ma).|2730+\-4 Ma (inferred)||||Fine- to medium-grained monzogranite; typically granophyric; metamorphosed|
34924|Butcher Bird Monzogranite|70794|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Youanmi Terrane, Yilgarn Craton.|2730+/-4 Ma|Of Marda Complex.|||Fine to medium grained monzogranite; typically granophyric; metamorphosed|
34924|Butcher Bird Monzogranite|71168|5|Briefly described|p7, p58, p60|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c. 2730 Ma|||||
34924|Butcher Bird Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
34924|Butcher Bird Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Of Marda Complex. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma); Youanmi Terrane events (3131 - 2600 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv.|2730+\-4 Ma||||Fine- to medium-grained monzogranite; typically granophyric; metamorphosed|
34924|Butcher Bird Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Youanmi Terrane.|2730+/-4 Ma|Marda Complex|||Fine- to medium-grained monzogranite; typically granophyric; metamorphosed.|
34924|Butcher Bird Monzogranite|73596|6|Mentioned|p1166, 1170|Neoarchean|Neoarchean|Southern Cross Domain, Youanmi Terrane. Appears descriptively as Butcher Bird granophyric monzogranite on p1166.|2730 +/- 4 Ma.|Polelle Group.||Intrudes Glen Group.||
23447|Butchers Gully Member|22496|6|Mentioned|p7|Orosirian|Orosirian|Age: 1848 +/- 3 Ma. Of the Olympio Formation.  Geological Province: Halls Creek Province.||||||12-AUG-04
23447|Butchers Gully Member|22526|5|Briefly described|P680, Fig3 P682||Orosirian|Age of unit is 1848+/-3 Ma||||||
23447|Butchers Gully Member|22547|5|Briefly described|P8|Orosirian|Orosirian|Of the Halls Creek Group. Age: 1857-1848 Ma.||||||14-NOV-06
23447|Butchers Gully Member|22754|4|Described|p3|Paleoproterozoic|Paleoproterozoic|Of the Olympio Formation.  Previously included in the Biscay Formation.  Age: 1848+/-3Ma (SHRIMP).||||||07-NOV-08
23447|Butchers Gully Member|22777|5|Briefly described|Map|||||||||
23447|Butchers Gully Member|23383|5|Briefly described|p12|Paleoproterozoic|Paleoproterozoic|Of the Olympio Formation (Halls Creek Group).  Contains the mineralised  "Nobium Tuff". Age: 1870+/-4Ma.||||||07-NOV-08
23447|Butchers Gully Member|23599|4|Described|p9|Paleoproterozoic|Paleoproterozoic|Of Olympio Formation. Geological Province: Lamboo Complex.||||||07-NOV-08
23447|Butchers Gully Member|23621|2|Defined|p51 Appendix|Orosirian|Orosirian|See also page 16, 11 table 1. Age: 1848+/-3 Ma. Of Olympio Formation. Underlying unit Biscay Formation. Geological Province: Halls Creek Orogen. Max. thickness: >1000 m.||||||
23447|Butchers Gully Member|23622|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Halls Creek Group.||||||07-NOV-08
23447|Butchers Gully Member|23897|6|Mentioned|p394 Tb.7|||Of Olympio Formation.||||||
23447|Butchers Gully Member|24173|3|Fully described|p17, p13 Tb.2|Paleoproterozoic|Paleoproterozoic|Of Olympio Formation. Contains the basal section informally referred to as  "Niobium tuff". Geological Province: Halls Creek Orogen. Max Thickness: >1000m. Age: 1848 +/- 3Ma.||||||09-DEC-08
23447|Butchers Gully Member|24572|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Olympio Formation.  Age: >1835Ma.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
23447|Butchers Gully Member|42768|6|Mentioned|p7|||of Olympio Formation.||||||
23447|Butchers Gully Member|43303|5|Briefly described|Map Legend||Paleoproterozoic|of Halls Creek Group.||||||07-NOV-08
23447|Butchers Gully Member|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Olympio Formation (Halls Creek Group). Metamorphosed and altered trachytic and trachyandesitic volcanic and volcaniclastic rock; chloritic with a carbonate-rich matrix; ferruginous chert. Age: c.1855Ma. In the Lamboo Complex (eastern)||||||07-NOV-08
23447|Butchers Gully Member|44693|5|Briefly described|Map Legend||Proterozoic|||||||
23447|Butchers Gully Member|50437|5|Briefly described|p1.7, 3.1, 5.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Butchers Gully Suite. Age: 1848-1857 +/- 5Ma (Shrimp).||||||07-NOV-08
23447|Butchers Gully Member|50542|5|Briefly described|p105|Paleoproterozoic|Paleoproterozoic|Of the Olympio Formation (Blake et al., 1999). Geological Province: Halls Creek Orogen.||||||07-FEB-11
23447|Butchers Gully Member|60724|4|Described|p8, p5 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Olympio Formation (Halls Creek Group). Consists of intermediate trachyandesitic volcanics and associated metasedimentary rocks; with well preserved volcanic structures such as pillows and pillow breccias. Age: 1.87Ga. Within the Lamboo Complex.||||||07-NOV-08
23447|Butchers Gully Member|63866|5|Briefly described|p130|||Ages are maximum depositional ages based on detrital zircons from the Olympio Formation.|c. 1857 and c. 1848 Ma.|Olympio Formation|||Pillow lavas, chert and trachytic volcanics.|
23447|Butchers Gully Member|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Of Olympio Formation. Metamorphosed and altered trachytic and trachyandesitic volcanic and volcaniclastic rock with carbonate-rich matrix; chert and ferruginous chert.||||||09-DEC-08
23447|Butchers Gully Member|66846|5|Briefly described|p549 Fig.2|Orosirian|Orosirian|In the Eastern Zone of the Lamboo Complex.||Olympio Formation||Coeval with Maude Headley Volcanic Member.|Alkaline volcanic rocks.|
23447|Butchers Gully Member|67127|4|Described|p85-87|Palaeoproterozoic|Palaeoproterozoic|The ""Niobium Tuff"" is a fluorite-bearing volcaniclastic unit at the base of this member that hosts polymetallic mineralisation called the Brockman deposit. Trachytic ash-flow tuff is composed of two closely spaced units from different eruptive episodes; a crystal-rich lower unit and an overlying pumice-rich unit. Varies in thickness from 5 to 35m and crops out for at least 3.5km. Sub-surface data shows this unit thicknes down dip to the east. Petrography is discussed. Additional zircon dates includes 1870 +/- 4 Ma (Taylor et al, 1995b) and 1868 +/- 3 Ma (Blake et al, 1999).|1848 +/- 3 Ma (SHRIMP, Blake et al., 1999)|Olympio Formation|||Volcaniclastic rocks, lava sequences and trachytic ash-flow tuff.|
23447|Butchers Gully Member|68078|6|Mentioned|p7 figure 4|Paleoproterozoic|Paleoproterozoic||1850-1860 Ma|Olympio Formation||||
23447|Butchers Gully Member|68656|5|Briefly described|GEOL_LUT_CSV/500k_geologyp08_lut|Paleoproterozoic|Paleoproterozoic|||Olympio Formation|||Metamorphosed and altered trachytic and trachyandesitic volcanic and volcaniclastic rock with carbonate-rich matrix; chert and ferruginous chert.|
23447|Butchers Gully Member|69003|5|Briefly described|p19|Paleoproterozoic|Paleoproterozoic|E zone, Lamboo Province, Halls Creek Orogen.||Olympio Formation.||||
23447|Butchers Gully Member|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Data from OZCHRON1. Comments: (1848 Ma)'This is the crystallisation age of the large broken zircons in this rock. It is based on 29 of the 30 data points. (1857 Ma) 'This igneous crystallisation age for the volcanic zircons is based on all 24 concordant data points.|1848+/-3 Ma, 1857+/-2 Ma U/Pb SHRIMP|Olympio Formation|Includes unnamed subunit.||Meta-andesitic to metatrachytic volcanic and volcaniclastic rocks with carbonate-rich matrix, and metachert and ferruginous metachert.|30-JUL-15
23447|Butchers Gully Member|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv. |1857 Ma||||Meta-andesitic to metatrachytic volcanic and volcaniclastic with carbonate rich matrix, metachert and ferruginous metachert.|
23447|Butchers Gully Member|69587|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|||Unit of Olympio Formation.|||Metamorphosed and altered trachytic and trachyandesitic volcanic and volcaniclastic rock with carbonate-rich matrix; chert and ferruginous chert|
23447|Butchers Gully Member|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|1848-1848 Ma (Inferred)|Unit of Olympio Formation.|||Meta-andesitic to metatrachytic volcanic and volcaniclastic rocks with carbonate-rich matrix, and metachert and ferruginous metachert, metatrachytic lava flows, domes, and sills.|
23447|Butchers Gully Member|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv.|1848 Ma|Olympio Formation|||Meta andesitic to metatrachytic volcanic and volcaniclastic rocks with carbonate rich matrix, metachert. Metatrachytic lava flows, domes and sills.|
23447|Butchers Gully Member|70812|5|Briefly described|p19|||Eastern Zone of the Lamboo province.|c. 1850 Ma|Olympio Formation.|||Trachyandesitic volcanic rocks.|
23447|Butchers Gully Member|71113|5|Briefly described|p96-98|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen. Zircon age dating of 1848+\-3 Ma (Blake et al., 1998).|1857 +/- 5 Ma (Page and Hancock, 1988)|Unit of Olympio Formation.|||Trachyandesitic and trachytic rocks.|21-AUG-19
23447|Butchers Gully Member|71140|6|Mentioned|p96, 98|Orosirian|Orosirian|Eastern Zone, Lamboo Province, Halls Creek Orogen.|1848 +/- 3 Ma (Blake et al., 1998).|Olympio Formation.||||
23447|Butchers Gully Member|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv and geochron files.|1846+\-4 Ma (isotopic)|Unit of Olympio Formation.|||Meta-andesitic to metatrachytic volcanic and volcaniclastic rocks with carbonate-rich matrix, and metachert and ferruginous metachert, metatrachytic lava flows, domes, and sills|
23447|Butchers Gully Member|71397|4|Described|p4-5,7,16,18,32,38,40-42,44,46,48|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen. Nomenclature of Griffin and Tyler (1993). Occurs between packages of thick-bedded turbidite metasandstone and metasiltstone; discrete volcanic centre of submarine alkaline lavas and associated volcaniclastic unit punctuating deep-marine sedimentation. Taylor et al. (1995a,b) divided the lavas into two compositional and textural types: 1) leucocratic, trachytic and amygdaloidal (amygdales filled with secondary limonite, calcite, biotite, quartz and/or fluorite); and 2) mesocratic, trachytic, pillowed or massive with some scoriaceous tops and interflow breccia beds. Sample GA 87598001 (fine-grained volcaniclastic rock) yielded a weighted mean 207Pb*/206Pb* date of 1868+\-5 Ma. Sample GA 87598002 (fine-grained volcaniclastic rock) yielded a weighted mean 207Pb*/206Pb* date of 1868+\-5 Ma. These ages were previously interpreted as age of the magmatic component (Taylor 1995b), but are reinterpreted here as detrital component as these ages are older than the underlying c. 1856 Ma Maude Headley Member. Sample GA 87598023 (trachytic lava) yielded 207Pb*/206Pb* dates of c. 3256, 3408 and 2637 Ma, interpreted as xenocrystic zircons. Sample GA 92524993c (amygdaloidal trachytic lava) yielded a weighted mean 207Pb*/206Pb* date of 1846+\-5 Ma, interpreted as age of volcanism.|1846+\-4 Ma|Unit of Olympio Formation.|||Metamorphosed andesitic to trachytic volcanic and volcaniclastic rocks with a carbonate-rich matrix.|
23447|Butchers Gully Member|71873|6|Mentioned|p426,443|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province.|||||Andesite, trachyte.|
23447|Butchers Gully Member|72437|5|Briefly described|p8, p24, p54|||Date range is derived from SHRIMP U-Pb dating by Page and Sun (1994) and Page, R.W. (1996, pers. Comm.). A SHRIMP U-Pb age of 1870 +/- 4 Ma is reported by Taylor et al (1995b) for a tuff unit and probably reflects detrital zircon and not magmatism. Eight whole-rock analyses are provided.|c. 1855-1845 Ma|Olympio Formation|||Alkaline volcanic and volcaniclastic rocks and minor basaltic rocks.|
77933|Butchers Well Basalt|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||2820 - 2711 Ma (inferred).||||Basalt; fine grained with local pyroxene-spinifex texture; minor interflow sedimentary rocks; metamorphosed.|
77933|Butchers Well Basalt|70326|3|Fully described|p336,338-9,341,343,346-7,351,353-4, p363|Neoarchean|Neoarchean|Geological province: Agnew region, Ora Banda Domain, Kalgoorlie Terrane, Yilgarn Craton. [Also referred to as Butchers Basalt on p343]. Subaqueous extrusive tholeiitic basalt that is highly fractionated (low-Mg#) and moderately enriched. Thickness: ?over 100m. Only occurs in sporadic outcrops on Western limb. Intruded at base by granite. Major and trace element geochemical analysis on Table 4 p342-346. Interpreted to be part of Cycle 0 of Agnew Greenstone Belt volcanism >2770-2830 Ma. See also p359,360,363.||||Overlain by Lawlers Tonalite.|High-Fe tholeiite to tholeiitic dacite: light green massive basalt, as submarine sheet flows?|29-JUL-19
77933|Butchers Well Basalt|71212|5|Briefly described|intro p2, intro p3|||Yilgarn Craton. ||||Overlain by the Donegal Komatiite.||
77933|Butchers Well Basalt|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2820-2711 Ma (inferred)||||Basalt; fine grained with local pyroxene-spinifex texture; minor interflow sedimentary rocks; metamorphosed|
77933|Butchers Well Basalt|73151|5|Briefly described|p3|Neoarchean|Neoarchean|Yilgarn Craton. Kalgoorlie Terrane, Agnew Greenstone Belt.||Kalgoorlie Group||Underlies Donegal Komatiite.|Basalt.|
77933|Butchers Well Basalt|73596|6|Mentioned|p1151-1152, 1156-1157, 1161-1163, 1167|||Lawlers Domain, Agnew-Wiluna Greenstone Belt. Deep-water mafic-ultramafic lava fields and feeder intrusions. Has been intruded by voluminous felsic plutons.||||Is overlain by Donegal Komatiite.||
27667|Buttons Formation|13194|4|Described|p391 Tb. 4-16, p402 fig 4-66|Famennian|Famennian|Type Section: near Buttons Crossing 15o37'S 128o42'E. 300-350m thick back-reef facies.||Ningbing Group||Overlies Hargreaves Formation (unconformably). Laterally equivalent to Garimala Limestone.|Sandy and fossiliferous limestones.|
27667|Buttons Formation|13234|6|Mentioned|p250 Fig.2, p252 Fig.4, |||||||||
27667|Buttons Formation|40792|6|Mentioned|Fig.3|||||||||
27667|Buttons Formation|40993|6|Mentioned|p7|||||||||
27667|Buttons Formation|41492|5|Briefly described|p114|||||||||
27667|Buttons Formation|41731|6|Mentioned|Fig.2|||||||||
27667|Buttons Formation|41839|6|Mentioned|p28|||||||||
27667|Buttons Formation|41864|2|Defined|p96|late Famennian||Age latest Famennian.||||||
27667|Buttons Formation|41865|5|Briefly described|Map legend||late Famennian|Age latest Famennian||||||
27667|Buttons Formation|42030|5|Briefly described|p750|||||||||
27667|Buttons Formation|42175|5|Briefly described|p197|||See also Fig.2||||||
27667|Buttons Formation|42547|5|Briefly described|p98|||||||||
27667|Buttons Formation|60364|4|Described|p184, 186, 192|Famennian|Famennian|Disconformably overlain by Burt Range Fm. Sandy and silty limestone with minor silty dolomite and sandstone with thin beds of sandy limestone. Richly fossiliferous. Thickness: >350m. Equivalent in part to Ningbing Gp. Geological Province: Bonaparte Basin.||||||17-MAR-08
27667|Buttons Formation|60682|5|Briefly described|p25 Fig. 22|Famennian|Famennian|?Of Ninbing Group. Interfingers with Ninbing Limestone. Geological Province: Bonaparte Basin.||||||17-MAR-08
27667|Buttons Formation|61542|5|Briefly described|p281-282 Figs. 7&8|Devonian|Devonian|||||||07-FEB-11
27667|Buttons Formation|64580|6|Mentioned|map legend|||Of Ningbing Group.||||||15-DEC-08
27667|Buttons Formation|64694|5|Briefly described|p232, p233, p234, p246, p253|Famennian|Famennian|Onshore Bonaparte Basin.||Unit in Ningbing Group.||Disconformably overlies Cockatoo Group. Is overlain by Langfield Group.||
27667|Buttons Formation|66127|6|Mentioned|p442.|Famennian|Famennian|Bonaparte Basin. Contains similar miospore assemblage (Playford, 1982) and ostracod fauna (Jones, 1985, 1987) to lower Fairfield Group, Canning Basin. ||||||
27667|Buttons Formation|69099|5|Briefly described|500k_geologyp08_lut.csv|Late Devonian|Late Devonian|||Ningbing Group||||
27667|Buttons Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Famennian|Frasnian|||||||
27667|Buttons Formation|69452|4|Described|p36:6 Fig.36.5; 36:7, 9-12|Famennian|Famennian|Mory and Beere (1988). Equivalent to Buttons Beds of Veevers and Roberts (1968) and Buttons beds of Playford (1982). The only unit in the Ningbing Group recognised in NT where the Group is entirely subsurface; the rest is undivided. Crops out in WA in the Burt Range area. Stratigraphic equivalent of Garimala Limestone. Lagoonal to ?back reef deposits. Up to 350m thick. Onshore.||Ningbing Group.||Overlies undivided Ningbing Group conformably and Cockatoo Group unconformably. Is overlain unconformably by Langfield Group and (locally) Milligans Formation.|Thinly bedded limestone (wackestone, grainstone, calcimudstone) and cross-bedded sandstone, with sandy and laminated carbonate beds.|12-JUL-16
27667|Buttons Formation|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Ningbing Group.||||
27667|Buttons Formation|69673|6|Mentioned|p169, p170 fig 142|||||Ningbing Group||Overlies Garimala Limestone, overlain by Langfield Group, Milligans Formation||
27667|Buttons Formation|71146|5|Briefly described|p6,  p43 fig 33|Famennian|Famennian|Bonaparte Basin.||||Overlies the Ningbing Group. Overlain by the Langfield Group.|Carbonate and mudstone.|
80993|Byro Group, lower|72034|5|Briefly described|500k_interpgeop16_lut|Kungurian|Artinskian|Southern Carnarvon Basin.  Age from biostratigraphy.||Byro Group|||Fine-grained, bioturbated sandstone overlying interbedded sandstone, siltstone, and mudstone.|
80994|Byro Group, middle|72034|5|Briefly described|500k_interpgeop16_lut|Kungurian|Kungurian|Southern Carnarvon Basin.  Age from biostratigraphy.||Byro Group|||Black shale and siltstone overlain by fine-grained sandstone; hummocky and swaley cross-stratified.|
80995|Byro Group, upper|72034|5|Briefly described|500k_interpgeop16_lut|Kungurian|Kungurian|Southern Carnarvon Basin.  Age from biostratigraphy.||Byro Group|||Intercalated siltstone, shale, and sandstone.|
41597|Bywash Formation|24544|5|Briefly described|p48|Paleoproterozoic|Paleoproterozoic|Of Capricorn Group. Geological Province: Ashburton Province.||||||07-NOV-08
41597|Bywash Formation|60301|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Blair Basin. Of the Capricorn Group. Age: c. 1804Ma. Sandstone, dolomitic sandstone, dolostone, dololutite, dolorudite and felsic volcanics.||||||17-AUG-04
41597|Bywash Formation|63866|5|Briefly described|p154|||Blair Basin. ||Capricorn Group|Includes the Koonong Member|Overlain by the Mooline Formation.||
41597|Bywash Formation|63869|4|Described|p7-8, p14, p53-54, p55, Plate 1|Paleoproterozoic|Paleoproterozoic|Named after Bywash Bore on central CAPRICORN sheet. 400-550 m thick. Paleoflow direction to NE. Lithology described in some detail.||Lower unit in Capricorn Group.|Includes Koonong Member.|Unconformably overlies Ashburton Formation. Is overlain conformably by Mooline Formation.|Thin- to very thick-bedded sandstone, dolomitic sandstone, dolostone, siltstone and felsic volcanic rock.|
41597|Bywash Formation|65830|6|Mentioned|Plate 2|Statherian|Orosirian|Blair Basin.||Of the Capricorn Group.||||
41597|Bywash Formation|66299|6|Mentioned|p202.|||||Unit in Capricorn Group.||Marked angular unconformity with underlying Ashburton Formation.||
41597|Bywash Formation|69024|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Blair Basin. Also includes an unnamed sub-unit.||Of the Capricorn Group.|Includes the Koonong Member.|Overlies Ashburton Formation unconformably. Overlain by the Mooline Formation.|Thin to very thick bedded medium to very coarse grained sandstone, dolomitic sandstone, dolostone, dololutite, dolorudite and felsic volcanic rock; siltstone, dolostone and fine- to coarse-grained sandstone.|05-MAY-14
41597|Bywash Formation|69028|5|Briefly described|Map Legend|Orosirian|Orosirian|Ashburton and Blair Basins. Mapped with Mooline Formation as a single unit.|c. 1805 Ma|Of the Capricorn Group.|||Conglomerate, ferruginous and quartzitic sandstone, ferruginous siltstone and mudstone, dolostone, and felsic volcanic rock.|07-MAY-14
41597|Bywash Formation|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|||Capricorn Group|Includes Koonong Member||Thin to very thick bedded fine to very coarse grained sandstone, dolomitic sandstone, siltstone, dolostone, dololutite, dolorudite, and felsic volcanic rock|
41597|Bywash Formation|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_interpgeop_lut.csv, 148922.1.pdf West Australian Craton|1804-1738 Ma|Capricorn Group|Includes Koonong Member|Overlies Ashburton Formation|Thin- to very thick-bedded ferruginous lithic quartz sandstone and dolomitic sandstone; minor siltstone and dolomitic siltstone, dolostone, conglomerate, and felsic volcanic rock.|
41597|Bywash Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, crystalline dolostone/dolomite, dololutite, dolorudite|
41597|Bywash Formation|72259|6|Mentioned|p3|Orosirian|Orosirian||ca. 1805 Ma|||||
79241|Cadda Sequence|69297|6|Mentioned|p202, p204, p206|Middle Jurassic|Middle Jurassic|Perth Basin. Exhibits good organic richness and potential to generate gas. May be up to 400m thick. See also p207, p209, p223, p225, p236, p238.||||Overlies the Cattamarra Sequence. Overlain by the Yarragadee Sequence.||
79241|Cadda Sequence|70097|5|Briefly described|p4|Middle Jurassic|Early Jurassic|Houtman Sub-basin.||||||
79742|Caines Monzogranite|70775|5|Briefly described|p24 tbl 3, p54|Mesoarchean|Mesoarchean|Previously the Caines Well Granite. |c. 2990 +/- 5 Ma||||Monzogranite.|
79742|Caines Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|De Grey Superbasin.|2990+/-5 Ma.|Maitland River Supersuite|||Biotite(--hornblende) monzogranite; foliated; local xenoliths of granitic gneiss; metamorphosed.|
33443|Cajou Monzogranite|23485|4|Described|p20|Paleoproterozoic|Paleoproterozoic|Age: 1961 +/- 3Ma (SHRIMP U-Pb zircon).||||||07-NOV-08
33443|Cajou Monzogranite|23486|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: c.1960 Ma.||||||07-NOV-08
33443|Cajou Monzogranite|66299|5|Briefly described|p105.|Proterozoic|Proterozoic|Gascoyne Province. Intrudes Archean granites of the Yilgarn Craton.|1961 +/- 3 Ma.||||Equigranular and porphyritic, medium-grained biotite monzogranite.|
79373|Calgra Member|72712|5|Briefly described|p9 Fig.5, p17, p19, p20 Fig.15.|Siderian|Siderian|New name. This unit previously included in the Meteorite Bore Member. The measured thickness is about 60 m in the type section on the northern limb of the Hardey Syncline. Also recognised on southern limb. Clasts smaller and less abundant than in Meteorite Bore Member. Basal contact sharp and conformable on Kungarra Formation, upper contact diffuse & assigned at the last observable glacial dropstone. Sample from underlying Kungarra Formation identified as younger than 2340+/- 22Ma, so dating of Calgra Member at < 2461+/-9 Ma says more about source materials than depositional age. Shown as CM on p20 Fig.15f. This is the upper of two glaciogenic horizons, the Meteorite Bore member being the lower. See also p36 Fig.25, p43 Fig.31, p17, p19, p35, p44, p47, p57.|< 2340 +/-22 Ma from underlying strata.|Upper Kungarra Formation||Shown as underlying Anthiby Formation (unconformably). Balgara Dolerite also intrudes near this contact.|Glacial diamictite.|
25827|Callawa Formation|7433|4|Described|p25 Fig.2, p42, pp44-45, p52.|Cretaceous|Jurassic|Southern Canning Basin. Widespread unit of fluvial, coarse clastics. Contains an unconfined aquifer.||||Overlaps Jarlemai Siltstone and Wallal Sandstone; overlies Precambrian basement. Is disconformably overlain by Parda Formation and Anketell Sandstone, and locally by Frezier Sandstone.|Fluvial quartzose sandstone, cross-bedded; conglomerate, minor siltstone.|
25827|Callawa Formation|22717|5|Briefly described|P11, P12|Cretaceous|Jurassic|||||||
25827|Callawa Formation|22738|4|Described|8,10,13,16,18|Early Cretaceous|Late Jurassic|||||||
25827|Callawa Formation|22753|5|Briefly described|Fig.3 p585|Cretaceous|Cretaceous|||||||
25827|Callawa Formation|22801|5|Briefly described|P12, Table1 P8|Early Cretaceous|Jurassic|Equivalent to Frezier Sandstone||||||
25827|Callawa Formation|23414|5|Briefly described|Map Legend|Early Cretaceous|Jurassic|Canning Basin||||||
25827|Callawa Formation|23415|5|Briefly described|Map Legend|Cretaceous|Jurassic|Very fine- to coarse-grained sandstone, ferruginous towards base; siltstone and conglomerate interbeds; plant and trace fossils; mainly fluvial deposits. Geological province: Westralian Superbasin||||||07-JAN-08
25827|Callawa Formation|23575|5|Briefly described|Map Legend|Mesozoic|Mesozoic|||||||
25827|Callawa Formation|23583|5|Briefly described|Map Legend|Cretaceous|Jurassic|Overlain by Parda Formation. Underlain by Paterson Formation. Geological Province Westralian Super Basin.||||||26-JUL-07
25827|Callawa Formation|23585|4|Described|p24|Mesozoic|Mesozoic|Underlain by Eel Creek Formation. Overlain by Westralian Superbasin.||||||26-JUL-07
25827|Callawa Formation|23745|4|Described|p19|Cretaceous|Jurassic|Previously part of Paterson Formation. Geological Province: Canning Basin.||||||
25827|Callawa Formation|23757|4|Described|p16-17|Cretaceous|Jurassic|Unconformably overlies Jarlemai and Wallal Sandstones; upper parts onlap Nimingarra Iron Fm. Disconformable below Parda Fm. Geological Province: Westralian Superbasin. Max. thickness: 100 m. Detailed lithology provided.||||||07-JAN-08
25827|Callawa Formation|23758|4|Described|p12|Cretaceous|Jurassic|||||||
25827|Callawa Formation|24025|5|Briefly described|p16|Cretaceous|Jurassic|Geological Province: Carnarvon Basin.||||||
25827|Callawa Formation|24110|5|Briefly described|Plate 1|Cretaceous|Jurassic|Geological Province: Northern Carnarvon and Canning Basins||||||
25827|Callawa Formation|29853|6|Mentioned|Fig.55|||||||||
25827|Callawa Formation|30402|4|Described|Table 2|||||||||
25827|Callawa Formation|32979|6|Mentioned|p38|||Correlation with basins in India||||||
25827|Callawa Formation|33164|6|Mentioned|p90|||Refers Veevers & Wells (1961)||||||
25827|Callawa Formation|33166|6|Mentioned|p67|||Stratigraphy||||||
25827|Callawa Formation|33939|6|Mentioned|p393|||U.Jur. - L.Cret.  Flora.||||||
25827|Callawa Formation|33965|6|Mentioned|Table 1|||||||||
25827|Callawa Formation|34363|6|Mentioned|p56|||Oxfordian. See Fig.7.||||||
25827|Callawa Formation|35127|6|Mentioned|Map legend|Early Cretaceous|Jurassic|||||||
25827|Callawa Formation|35201|6|Mentioned|Map legend|Cretaceous|Jurassic|||||||
25827|Callawa Formation|35202|6|Mentioned|Map legend|Early Cretaceous|Jurassic|||||||
25827|Callawa Formation|35207|6|Mentioned|Map legend|Early Cretaceous|Jurassic|||||||
25827|Callawa Formation|35222|4|Described|Table.2|||||||||
25827|Callawa Formation|35223|4|Described|Table.2|||||||||
25827|Callawa Formation|35225|4|Described|Table 1|||||||||
25827|Callawa Formation|35226|4|Described|Table 1|||||||||
25827|Callawa Formation|35251|6|Mentioned|Map legend|Early Cretaceous|Jurassic|||||||
25827|Callawa Formation|35252|6|Mentioned|Map legend|Early Cretaceous|Jurassic|||||||
25827|Callawa Formation|35497|4|Described|Table 1|||Also on p10.||||||26-JUL-07
25827|Callawa Formation|35711|6|Mentioned|p27|||See also Table 3,stratigraphy.||||||
25827|Callawa Formation|35902|6|Mentioned|p10|||||||||
25827|Callawa Formation|35903|6|Mentioned|p7|||||||||
25827|Callawa Formation|35969|6|Mentioned|Table 7|||||||||
25827|Callawa Formation|36438|6|Mentioned|Map legend|Early Cretaceous|Jurassic|Jurassic to Early Cretaceous||||||
25827|Callawa Formation|36632|6|Mentioned|Map legend|Early Cretaceous|Jurassic|Jurassic to Early Cretaceous.||||||
25827|Callawa Formation|36890|6|Mentioned|p349|||||||||
25827|Callawa Formation|37368|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
25827|Callawa Formation|37370|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
25827|Callawa Formation|37564|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
25827|Callawa Formation|38878|6|Mentioned|Map legend|Aptian|Tithonian|Tithonian - Aptian||||||
25827|Callawa Formation|39697|6|Mentioned|p138|||||||||
25827|Callawa Formation|39857|6|Mentioned|Map legend|Late Cretaceous|Late Jurassic|Early Cretaceous to Late Jurassic||||||
25827|Callawa Formation|43563|6|Mentioned|Fig.2,p5||Early Cretaceous|||||||
25827|Callawa Formation|43656|6|Mentioned|Fig.2,p8|Barremian|Berriasian|||||||
25827|Callawa Formation|43746|6|Mentioned|Fig.2,p11|Barremian|Berriasian|||||||
25827|Callawa Formation|44143|4|Described|p.432 Table 4-19; p.449, Figure 4-108|Cretaceous|Jurassic|Up to 80m thick; very fine to coarse sandstone, conglomerate; fluvial. Unconformably overlies Paterson Formation, Poole Sandstone, Noonkanbah Formation & Triwhite Sandstone; disconformably or unconformably overlies Jarlemai Siltstone & Wallal Sandstone. Type section in hills NW of Callawa homestead (YARRIE: 20deg 32' S, 120deg 21' E).||||||22-NOV-17
25827|Callawa Formation|44189|5|Briefly described|Map legend|Cretaceous|Jurassic|||||||
25827|Callawa Formation|44229|5|Briefly described|Map Legend|Cretaceous|Jurassic|Very fine- to coarse-grained sandstone,ferruginous towards base; siltstone and conglomerate interbeds; plant and trace fossils.||||||10-NOV-04
25827|Callawa Formation|44356|6|Mentioned|p10||Late Jurassic|||||||
25827|Callawa Formation|44357|4|Described|p13,Tb.1 p8||Jurassic|Crops out in SW corner of sheet area.||||||
25827|Callawa Formation|44443|5|Briefly described|map legend|Early Cretaceous|Late Jurassic|||||||
25827|Callawa Formation|44479|2|Defined|p.8|||E/51-1. In undifferentiated Mesozoic abundant plants.||||||
25827|Callawa Formation|44480|14|Not recorded|map legend|||||||||
25827|Callawa Formation|44692|14|Not recorded|p.20|||||||||
25827|Callawa Formation|44998|1|Redefined|p.120-1|||Overlain by Anketell Formation. On many pages. p.78,119,122-130-3,5,143,151-5,6,7,160-4,6,184,189, App.6 p291,297.||||||
25827|Callawa Formation|45149|6|Mentioned|p56|||||||||
25827|Callawa Formation|45153|2|Defined|App.6-112|Late Jurassic|Late Jurassic|Previously Callawa Boulder beds (Reeves,51) Callawa beds(Fairbridge,53).||||||09-DEC-08
25827|Callawa Formation|45158|3|Fully described|p14|||See also pp11 and 13.||||||26-JUL-07
25827|Callawa Formation|45923|14|Not recorded|p.71,72||Jurassic|||||||
25827|Callawa Formation|46319|4|Described|p18|Late Jurassic|Late Jurassic|Maximum thickness: 100m.  Geological Province: Canning Basin.||||||
25827|Callawa Formation|48826|14|Not recorded|Tb.III|||Part correlates with Culvida Sandstone.||||||
25827|Callawa Formation|50189|5|Briefly described|p7|Cretaceous|Jurassic|Consists of upper and lower section; basal conglomerate, claystone, sandstone, conglomerate. Unconformably overlies: Paterson Formation; unconformably onlaps Nimingarra Iron Formation. Geological Province: Lambert Shelf.||||||
25827|Callawa Formation|50302|5|Briefly described|Map Legend|Cretaceous|Jurassic|Coarse-grained sandstone; siltstone and conglomerate interbeds.  Geological Province: Northern Carnarvon Basin.||||||09-JUN-04
25827|Callawa Formation|50383|5|Briefly described|Map Legend|Cretaceous|Jurassic|Geological Province: Northern Carnarvon Basin, Westralian Basin.||||||23-JUN-04
25827|Callawa Formation|50544|3|Fully described|p64, p16 Tb. 1|Early Cretaceous|Late Jurassic|Cliff-forming unit, comprising lower and upper sections.  Unconformably overlies Paterson Formation, Gorge Creek and De Grey Groups, and Eel Creek Formation.  Age: 150.7-120.5Ma.  Geological Province: Canning and Northern Carnarvon Basins.  See also p14.||||||
25827|Callawa Formation|50555|5|Briefly described|Map legend|Cretaceous|Jurassic|Very fine to coarse-grained sandstone, ferruginous towards base,with siltstone and conglomerate interbeds; plant and trace fossils.  Geological Province: Canning and Northern Carnarvon Basins (Westralian Superbasin).||||||21-JUL-04
25827|Callawa Formation|60429|4|Described|p7, p27-28|Cretaceous|Jurassic|Unconformably overlies Paterson and Eel Creek Formations; upper part unconformably onlaps the Nimingarra iron Fm. Max. thickness: ~100m. Comprises lower and upper sections of which considerable lithological details are presented. See also p8 Fig. 4.||||||07-FEB-11
25827|Callawa Formation|63420|5|Briefly described|Map legend|Cretaceous|Jurassic|Very fine- to coarse-grained sandstone; minor conglomerate.||||||
25827|Callawa Formation|64580|4|Described|map legend|Early Cretaceous|Early Cretaceous|Very fine- to coarse-grained sandstone, conglomerate.||||||09-DEC-08
25827|Callawa Formation|64643|5|Briefly described|p3 Fig. 2|Early Cretaceous|Early Cretaceous|||||||10-FEB-20
25827|Callawa Formation|65301|5|Briefly described|p5 Fig. 4|Early Cretaceous|Early Cretaceous|Geological province: Canning Basin.||||||
25827|Callawa Formation|65449|5|Briefly described|p6|Early Cretaceous|Early Cretaceous|||||Is overlain by Samuel Formation. Lateral equivalent of Broome Sandstone.||
25827|Callawa Formation|67202|4|Described|p43, p44 Fig.2.10, p69-71, p73, p118-119|Early Cretaceous|Late Jurassic|See also p126, p128, p134-135. One of the dominant aquifers in the Canning Basin. Over 80m thick; 52m thick at the type section. Fluvial deposits. Conductivity images.||||Unconformably overlies Poole Sandstone, Triwhite Sandstone and Broome Sandstone. Is overlain by Parda Formation, Frezier and Anketell Sandstones. Correlative of Cronin Sandstone.|Poorly sorted sandstone and conglomerate; minor siltstone.|15-FEB-18
25827|Callawa Formation|68007|5|Briefly described|p4, p8, Plate 1|Early Cretaceous|Early Cretaceous|Canning Basin. Fluvial deposits.||||Overlies Noonkanbah Formation, probably unconformably. Is overlain by Anketell Formation and (most probably) by Samuel Formation. Lateral equivalent of Broome Sandstone.||19-FEB-20
25827|Callawa Formation|68283|5|Briefly described|Map Legend|Cretaceous|Jurassic|Canning Basin.|||||Very fine to coarse-grained sandstone; minor conglomerate.|
25827|Callawa Formation|68902|6|Mentioned|p9 fig 5|Cretaceous|Cretaceous|||||Overlain by Samuel Formation.||
25827|Callawa Formation|69167|4|Described|geologyp_lut.csv|Early Cretaceous|Early Cretaceous||||||Very fine grained to coarse grained sandstone, conglomerate.|10-FEB-20
25827|Callawa Formation|69182|6|Mentioned|Ch4 p3, Ch4 p9, Ch4 p45, Ch4 p47|||Canning Basin. ||||Unconformably overlies the Jarlemai Siltstone. Overlain by the Samuel Formation.||
25827|Callawa Formation|69185|4|Described|GEOL_LUT_CSV files|Early Cretaceous|Early Cretaceous|Of Northern Carnarvon and Canning basins. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.||||Overlain by Frezier Formation.|Very fine- to coarse-grained sandstone, conglomerate|
25827|Callawa Formation|69590|4|Described|GEOL_LUT_CSV files|Early Cretaceous|Early Cretaceous|Of Canning Basin. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|145-101 Ma (inferred)||||Very fine grained to coarse grained sandstone, conglomerate|
25827|Callawa Formation|70774|5|Briefly described|p4|Early Cretaceous|Early Cretaceous|Willara and Kidson Sub-basins, Canning Basin.||||Unconformably overlies the Jarlemai Siltstone. Overlain by the Samuel Formation. Equivalent to the Broome Sandstone and Cronin Formation.||10-FEB-20
25827|Callawa Formation|70936|5|Briefly described|p60|Cretaceous|Jurassic|Geological province: Pilbara Craton.||||Underlain by Eel Creek Formation.||
25827|Callawa Formation|71003|6|Mentioned|p60|Cretaceous|Jurassic|Pilbara Craton.||||Overlies the Eel Creek Formation.||
25827|Callawa Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, siltstone, sandstone|
25827|Callawa Formation|71894|5|Briefly described|p4|Early Cretaceous|Early Cretaceous|Canning Basin.||||Unconformably overlies the Jarlemai Formation, Overlain by the Samuel Formation.|Sandstone, shale and conglomerate.|10-FEB-20
25827|Callawa Formation|72034|5|Briefly described|500k_interpgeop16_lut|Early Cretaceous|Early Cretaceous|Canning Basin; Roebuck Basin.|||||Very fine-grained to coarse-grained sandstone, and conglomerate.|
25827|Callawa Formation|72497|5|Briefly described|p3 Fig.2.|Barremian|Berriasian|Shown as occuring in the Anketell, Tabletop, Ryan Shelves, Willara and Kidson Sub-basin.||||Conformably underlies Samuel Formation and is laterally equivalent to Cronin Formation. Unconformably overlies Jarlemai Siltstone.||
25827|Callawa Formation|72499|5|Briefly described|p7 Fig.6.|Early Cretaceous|Early Cretaceous|Located in the Willara Sub-basin.||||Shown with Cronin Formation as unconformably overlying Jarlemai Formation, underlies Samuel Formation and is laterally equivalent to Broome Sandstone.||
25827|Callawa Formation|73117|5|Briefly described|p3|Lower Cretaceous|Lower Cretaceous|Canning Basin. Lower boundary[?] marked by the Breakup Unconformity that represents Jurassic-Cretaceous extensional events offshore.||||Unconformably underlain by Jarlemai Siltstone. Overlain by Samuel Formation. Equivalent to Cronin Formation and Broome Sandstone.|Dominantly sandstone with lesser shale and conglomerate in the lower portion[?].|
25827|Callawa Formation|73445|5|Briefly described|p3, 6, 8, 12, 24, 36-37, 41-46, 65-118|Mesozoic|Mesozoic|Playford et al. (1975). Canning Basin.||||Unconformably overlies Noonkanbah Formation locally.|Sandstone and conglomerate.|
25827|Callawa Formation|73574|5|Briefly described|p761-763|Valanginian|Valanginian|Northern Pilbara Craton, unconformably overlies granite-greenstone bedrock.||||Unconformably overlies Poole Sandstone, underlies Frezier Sandstone|Fluvial cross-bedded sandstone, conglomerate and minor siltstone; contains plant and trace fossils.|
68674|Callina Supersuite|61253|5|Briefly described|p52 Fig. 2, p56|Archean|Archean|Intrusive tonalite-trondhjemite-granodiorite magmas forming a sheeted sill complex with local crustal thickening and development of volcanic domes.  Age: 3490-3450Ma. Geological Province: eastern Pilbara Craton. See also p54-55 Fig. 3.||||||07-NOV-08
68674|Callina Supersuite|63417|5|Briefly described|Map legend|Archean|Archean|Includes Underwood Gneiss and Homeward Bound Granite. Geological Province: Pilbara Craton.||||||07-NOV-08
68674|Callina Supersuite|63420|5|Briefly described|Map legend|Archean|Archean|Includes Motherin Monzogranite and four unnamed granitic units.  Ages range through c.3469Ma, 3475Ma and 3470Ma.Geological Province: Pilbara Craton.||||||07-NOV-08
68674|Callina Supersuite|63441|4|Described|p35, p7 Tb. 2, p30|Archean|Archean|Part of structural Warrawaginee Granitic Complex.Incl: Motherin Monzogranite, Underwood + Wilson Well Gneisses. Age: 3490-3460Ma. Geol.prov:East Pilbara Terrane. Sodic metagranitic rocks/extensively migmatised (further lithology given).See also p31 Fig.10||||||07-FEB-11
68674|Callina Supersuite|63538|6|Mentioned|p6 Fig. 3|Archean|Archean|Geological Province: Pilbara Craton.||||||19-APR-13
68674|Callina Supersuite|64580|6|Mentioned|map legend|||||||||
68674|Callina Supersuite|64621|5|Briefly described|Map legend|Archean|Archean|Includes Owens Gully Diorite, Underwood Gneiss, Homeward Bound Granite and Coolyia Creek Granodiorite and 6 unnamed sub-units.  Ages from 3469 to c.3462Ma.||||||07-NOV-08
68674|Callina Supersuite|64654|5|Briefly described|Map Legend|Archaean|Archaean|Age: c. 3470Ma. Geological Province: Pilbara Craton. Hetrogeneous, migmatitic, tonalitic-granodioritic orthogeniss.||||||
68674|Callina Supersuite|64657|5|Briefly described|Map Legend|Archaean|Archaean|Age: c. 3470Ma. Geological Province: Pilbara Craton. 2 units comprising hetrogeneous, migmatitic, tonalitic-granodioritic orthogneiss and migmatitic-tonalitic orthogneiss, with abundant inclusions of amphiblite.||||||16-APR-13
68674|Callina Supersuite|64747|6|Mentioned|p115|Paleoarchean|Paleoarchean|Part of an East Pilbara-wide episode of voluminous felsic volcanic-plutonic activity.|3470-3460 Ma.||||Granitic.|
68674|Callina Supersuite|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|||Includes Homeward Bound Granite and Underwood Gneiss.|||
68674|Callina Supersuite|65827|4|Described|p1, p6 Tb.2, p9 Fig3, p15, p18, p22, p59|Paleoarchean|Paleoarchean|3490-3460 Ma. Of Mount Edgar Granitic Complex. Includes Underwood Gneiss, Homeward Bound Granite. Intruded by Chessman Granodiorite (Emu Pool Supersuite). Metamorphosed tonalite, trondhjemite, granodiorite, monzogranite, syenogranite and granitic gneiss.||||||21-MAY-14
68674|Callina Supersuite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Age of c.3469 - c.3459 Ma. Includes Coolyia Creek Granodiorite, North Shaw Tonalite, Owens Gully Diorite, Homeward Bound Granite, Underwood Gneiss, Motherin Monzogranite and North Pole Monzogranite.||||||
68674|Callina Supersuite|66217|4|Described|p5, p6 Table 1, pp10-15, p24.|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Predominantly sodic; derived from melting of basaltic protoliths. Emplaced as sheeted sill complex in greenstones contemporaneously with Warrawoona Group volcanism. The unit's tonalite-trondhjemite-granodiorite rocks are typical of Paleoarchean TTG and have a different source from Duffer Formation.|3490-3460 Ma.|Unit in Muccan, Yule, Shaw and Mount Edgar Granitic Complexes, and Carlindi Granitoid Complex.|Includes Homeward Bound Granite.|Intrudes Pilbara Supergroup. Is intruded by Apex Basalt feeder dykes.|Dominantly mafic granodiorite; hornblende diorite, migmatitic orthogneiss, gneissic tonalites and undeformed porphyritic monzogranites.|
68674|Callina Supersuite|67197|5|Briefly described|p5, p9, p14, p19, p22, p25, p29, p33-34|||See also p36. A component in the Carlindi Granitic Complex.|3490-3460 Ma.||||Granitic rocks.|
68674|Callina Supersuite|67201|6|Mentioned|p7 Fig.7|||East Pilbara Terrane.||||||
68674|Callina Supersuite|67269|5|Briefly described|p5|Paleoarchean|Paleoarchean||||||Tonalite and granodiorite.|
68674|Callina Supersuite|68035|5|Briefly described|p286 Fig 3|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Associated with Warrawoona Group.|3.53 - 3.46 Ga|||||
68674|Callina Supersuite|68280|6|Mentioned|p3|Paleoarchean|Paleoarchean||3530-3460 Ma|||||
68674|Callina Supersuite|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Detailed lithology discussed in map legend; the 5 facies are mapped separately.|c.3475 Ma and c.3469 Ma.||Includes the Motherin Monzogranite.||Metagranodiorite to metamonzogranite; biotite-hornblende quartz diorite and monzogranite; interleaved metamonzogranite, metagranodiorite, gneiss and pegmatite; interleaved seriate to porphyritic metamonzogranite, metagranodiorite and pegmatite.|02-DEC-14
68674|Callina Supersuite|68282|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. 6 facies are mapped separately.||||Includes sheets of Tambina Supersuite leucogranite.|Foliated meta hornblende diorite; partly melted orthogneiss; migmatitic orthogneiss with K-feldspar augen; migmatitic tonalitic orthogneiss and diatexite; heterogeneous migmatitic tonalitic to granodioritic orthogneisses.|
68674|Callina Supersuite|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Four other un-named facies are mapped separately. Ages from Buick et al. (1995), and Baker (2001) written communication.|c.3475-c.3469 Ma.||Includes Motherin Monzogranite.||Biotite-hornblende quartz diorite, monzogranite and granodiorite, all metamorphosed; migmatitic tonalitic orthogneiss and diatexite; interleaved metamonzogranite, metagranodiorite, granitic gneiss, and pegmatite.|06-JAN-15
68674|Callina Supersuite|69012|5|Briefly described|Map Legend|Archean|Archean|East Pilbara Terrane. Three unnamed sub-units are also mapped separately.|||Includes the North Shaw Tonalite and Coolyia Granodiorite.||Metagranodiorite, metatonalite, metadiorite, migmatitic orthogneiss and diatexite, intrusive sheets of leucogranite and/or leucosome.|28-APR-14
68674|Callina Supersuite|69013|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane. Includes 2 unnamed facies. Occurs as minor banded granitic gneiss within the Cleland Supersuite.|c.3475-c.3469 Ma||Includes the Motherin Monzogranite.||Metamonzogranite, metagranodiorite, pegmatite, gneiss.|29-APR-14
68674|Callina Supersuite|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Geochronology by Buick et al. (1995), Zegers (1996) and McNaughton et al. (1988). Also includes 6 unnamed sub-units mapped separately. See map legend for a detailed lithological description.|c.3484-c.3467 Ma.||||Metagranodiorite, metatonalite, orthogneiss, monzogranite.|01-MAY-14
68674|Callina Supersuite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Orthogneiss, tonalitic orthogneiss, granodioritic orthogneiss and migmatitic orthogneiss and diorite; metamorphosed. Biotite-hornblende metagranodiorite and metamonzogranite. |||Includes Owens Gully Diorite, Homeward Bound Granite, North Shaw Tonalite, Motherin Monzogranite, Underwood Gneiss, Homeward Bound Granite||Meta hornblende diorite, heterogenous migmatitic tonalitic to granodioritic orthogneiss with sheets of schlieric leucogranite. Porphyritic monzogranite, biotite-hornblende monzogranite, meta biotite monzogranite.|
68674|Callina Supersuite|69185|5|Briefly described|500k_geologyp08_lut.csv|||Geological Province: Pilbara Craton.|||Includes North Pole Supersuite.|||
68674|Callina Supersuite|69301|5|Briefly described|p5 Fig.3, p10-11|||Pilbara Craton. East Pilbara Terrane. Pilbara Supergroup successions include thick felsic volcanic formations, each contemporaneous with the four granitic supersuites. i.e. Duffer Formation and Callina Supersuite.|||Homeward Bound Granite||Felsic.|
68674|Callina Supersuite|69566|5|Briefly described|p236-237, 248|||Mount Edgar Granitoid Complex, East Pilbara Granite-Greenstone Terrane.|3469-3462 Ma.||Homeward Bound Granite, Underwood Gneiss, Owens Gully Diorite.||Voluminous TTG magmatism; gneisses.|
68674|Callina Supersuite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.|3493-3462 Ma (inferred; isotopic)||Includes North Shaw Suite, Homeward Bound Granite, Motherin Monzogranite, Owens Gully Diorite, Underwood Gneiss, Underwood Gneiss.|Interleaved with Mulgandinnah Monzogranite.|Bt-hbl monzogranite and quartz diorite, diorite; migmatitc, tonalitic to granodioritic orthogneiss.|
68674|Callina Supersuite|70022|6|Mentioned|p115|||East Pilbara Terrane.||||||
68674|Callina Supersuite|70775|5|Briefly described|p2, p69|Paleoarchean|Paleoarchean|These are some of the oldest exposed rocks in the Pilbara Craton.|c. 3484-3462 Ma||||Granites.|
68674|Callina Supersuite|70884|6|Mentioned|p122-123,135|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|3.49-3.46 Ga|||||
68674|Callina Supersuite|71041|6|Mentioned|p44, p45 fig 2||||3470 Ma||||Granitoid rocks.|07-NOV-17
68674|Callina Supersuite|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||monzogranite, granodiorite, granite, felsic gneiss|
68674|Callina Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||Max age 3484+/-4 Ma, min 3462+/-4 Ma.||Includes Owens Gully Diorite, Homeward Bound Granite, Coolyia Creek Granodiorite, North Shaw Tonalite, Underwood Gneiss, Motherin Monzogranite.||Metadiorite to metasyenogranite; massive to gneissic.|
68674|Callina Supersuite|72064|5|Briefly described|p79|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Intrusive felsic magmatism intruding into the East Pilbara Terrane. Interpreted to be derived from partial melting of basaltic crust with a contribution from older felsic magmatic components (Bickle et al., 1993).|3.49-3.46 Ga||||Tonalite¿trondhjemite-granodiorite granites.|28-JAN-20
68674|Callina Supersuite|72251|5|Briefly described|p52-54|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Contemporaneous with felsic extrusive units within the Duffer Formation. Granitic supersuite with Nd model age of ~4.1-3.4 Ga (Smithies et al., 2003, 2007; Champion, 2013).|3.49-3.46 G|||||
68674|Callina Supersuite|72668|6|Mentioned|p9-11, p13, p18-19, p25||Paleoarchean|Comagmatic with the eruption of the Duffer Formation.|c. 3490 Ma-3460 Ma||Includes North Shaw Suite.||Includes TTG granites.|12-JAN-22
68674|Callina Supersuite|73598|6|Mentioned|p1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.||||||
26448|Callytharra Formation|12471|6|Mentioned|p475 Fig.2.|Early Permian|Early Permian|Carbonates and muds.||||Overlies Lyons Group. Is overlain by Kennedy Group ?.||24-OCT-14
26448|Callytharra Formation|12731|6|Mentioned|p591 Fig.3.|||||||Overlies Lyons Group. Is overlain by Wooramel Group.||
26448|Callytharra Formation|12733|5|Briefly described|p554 Fig.2.|Early Permian|Early Permian|Sakmarian. Gaseous source in Merlinleigh Sub-basin and Byro Sub-basin.||||Overlies Lyons Group. Is overlain by Wooramel Group.|Predominantly clastic shallow marine deposits.|
26448|Callytharra Formation|13615|3|Fully described|p3-4, p6-p8, p15-p16|Artinskian|Sakmarian|Peedamullah Shelf. Up to 110m thick. Spores and Pollen zone provided. The type section is found in the Wooramel River on the South end of the Carrandibby Range; 25deg53'30"S 115deg30'00"E. Contains diverse and abundant fauna which form the basis of its age interpretation. Deposited in a marine shelf. See also p27, p34-p35, p42, p44, 53, 58, 76, 78, 79, p80, p103 , p118 App. 5, Plates 2, 3.||Of Lyons Group.?||Conformably overlies the Lyons Group. Unconformably overlain by the Kennedy Group.|Fossiliferous, grey to green calcareous siltstone with hard fossiliferous calcarenite.|07-FEB-19
26448|Callytharra Formation|14228|5|Briefly described|Cover, p7-8, p10, p14 fig 6, p15, p18|Permian|Permian|Merlinleigh Sub-basin. Abundantly fossiliferous.|||Winnemia Sandstone, and Ballythanna Sandstone, Members.|Laterally equivalent to Cordalia Formation. Overlies Lyons Group conformably. Overlain by Wooramel Group.|Siltstone, shale and limestone; local sandstone.|
26448|Callytharra Formation|22817|5|Briefly described|p2|Early Permian|Early Permian|Carnarvon Basin||||||
26448|Callytharra Formation|23174|5|Briefly described|Fig5p8|Permian|Early Permian|||||||
26448|Callytharra Formation|23310|5|Briefly described|Map legend|Sakmarian|Sakmarian|||||||
26448|Callytharra Formation|23311|5|Briefly described|map legend|Sakmarian|Sakmarian|||||||
26448|Callytharra Formation|23312|5|Briefly described|map legend|Sakmarian|Sakmarian|||||||
26448|Callytharra Formation|23403|4|Described|p7|Late Permian|Middle Devonian|||||||24-NOV-09
26448|Callytharra Formation|23569|4|Described|p4 Tb. 1|Early Permian|Early Permian|Parent: Lyons Group. Interbedded fossiliferous siltstone and limestone||||||11-APR-08
26448|Callytharra Formation|23620|5|Briefly described|p4 Fig. 4|Permian|Devonian|||||||
26448|Callytharra Formation|23726|5|Briefly described|p37|Early Permian|Early Permian|Overlying unit Moogooloo Sandstone. Underlying unit Carrandibby Formation. Geological Province: Byro Sub-basin.||||||
26448|Callytharra Formation|23815|4|Described|p280|Sakmarian|Sakmarian|Geological Province: Carnarvon Basin. Underlying Units: Carrandibby Formation and Lyons Group (both conformable). Overlying units: Wooramel Group (disconformable) and Moogooloo Sandstone. Max. thickness: 265 m. Extremely fossiliferous.||||||24-NOV-09
26448|Callytharra Formation|23976|5|Briefly described|Map Legend|Permian|Devonian|||||||
26448|Callytharra Formation|23977|5|Briefly described|Map Legend|Permian|Devonian|||||||
26448|Callytharra Formation|23978|5|Briefly described|Map Legend|Permian|Devonian|||||||
26448|Callytharra Formation|24044|5|Briefly described|p541 Fig.2|Early Permian|Early Permian|||||||
26448|Callytharra Formation|24059|5|Briefly described|p137|Permian|Permian|Geological Province: Exmouth Sub-basin.  Maximum thickness: 300m.||||||
26448|Callytharra Formation|24114|5|Briefly described|p5 Fig.4|||Geological Province: Carnarvon Basin.||||||
26448|Callytharra Formation|24390|5|Briefly described|p19 Fig. 10|Permian|Permian|Geological Province: Southern Carnarvon Basin.||||||
26448|Callytharra Formation|24410|5|Briefly described|p137 Fig. 80|Permian|Carboniferous|Of the Lyons Group. Limestone, conglomerate, sandstone and siltstone; glacigene and marine.||||||24-NOV-09
26448|Callytharra Formation|29548|6|Mentioned|p227|||||||||
26448|Callytharra Formation|29889|6|Mentioned|p141|||||||||
26448|Callytharra Formation|30545|6|Mentioned|Fig.2|||Sakmarian age. See also P22||||||
26448|Callytharra Formation|30550|6|Mentioned|p94|||Fauna.||||||
26448|Callytharra Formation|31396|6|Mentioned|p1183|||||||||
26448|Callytharra Formation|31561|5|Briefly described|p9|||See P32,34. Hydrocarbon potential. Stratigraphy. Sakmarian-Artinskian.||||||
26448|Callytharra Formation|32113|6|Mentioned|p47|||||||||
26448|Callytharra Formation|32648|6|Mentioned|p32|||L.Perm.||||||
26448|Callytharra Formation|32945|6|Mentioned|p73|||See also P88. Sakmarian||||||
26448|Callytharra Formation|33386|6|Mentioned|Fig.7|||||||||
26448|Callytharra Formation|33453|5|Briefly described|p70|||Sak-Artinsk.||||||
26448|Callytharra Formation|33594|6|Mentioned|p37|||||||||
26448|Callytharra Formation|33627|6|Mentioned|p582|||||||||
26448|Callytharra Formation|33701|6|Mentioned|Fig.1|||Sakmarian.||||||
26448|Callytharra Formation|33710|6|Mentioned|Table 1|||||||||
26448|Callytharra Formation|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
26448|Callytharra Formation|34475|6|Mentioned|p261|||||||||
26448|Callytharra Formation|34532|6|Mentioned|p220|||See also PP221,223,224,etc.||||||
26448|Callytharra Formation|34570|6|Mentioned|p114|||||||||
26448|Callytharra Formation|35059|6|Mentioned|p205|||||||||
26448|Callytharra Formation|35105|6|Mentioned|Fig.66|||||||||
26448|Callytharra Formation|35282|6|Mentioned|p3|||See also P19 and Fig.19.||||||
26448|Callytharra Formation|36257|6|Mentioned|Table 2.1|||||||||
26448|Callytharra Formation|36387|6|Mentioned|p185|||||||||
26448|Callytharra Formation|36890|3|Fully described|p280|||Formerly Callytharra Limestone||||||
26448|Callytharra Formation|37294|6|Mentioned|p100|||||||||
26448|Callytharra Formation|37295|6|Mentioned|p53|||See also Table 2.||||||
26448|Callytharra Formation|37549|6|Mentioned|p110|||||||||
26448|Callytharra Formation|37920|5|Briefly described|p453|||||||||
26448|Callytharra Formation|37925|6|Mentioned|p493|||||||||
26448|Callytharra Formation|38217|5|Briefly described|p269|||Fossil correlations||||||
26448|Callytharra Formation|38444|6|Mentioned|p300|||||||||
26448|Callytharra Formation|38493|3|Fully described|p34|||||||||
26448|Callytharra Formation|38586|6|Mentioned|p29|||||||||
26448|Callytharra Formation|38917|6|Mentioned|p159|||See also P169||||||
26448|Callytharra Formation|39223|6|Mentioned|p238|||||||||
26448|Callytharra Formation|39263|6|Mentioned|p152|||||||||
26448|Callytharra Formation|39316|6|Mentioned|Fig.2|||||||||
26448|Callytharra Formation|39370|4|Described|p34|||See also P3||||||
26448|Callytharra Formation|39427|4|Described|Table 1|||||||||
26448|Callytharra Formation|39615|6|Mentioned|p83|||||||||
26448|Callytharra Formation|39865|6|Mentioned|p18|||||||||
26448|Callytharra Formation|40336|6|Mentioned|p18|||||||||
26448|Callytharra Formation|40339|6|Mentioned|Map legend|Permian|Permian|||||||
26448|Callytharra Formation|40340|6|Mentioned|Table 2|||||||||
26448|Callytharra Formation|40343|6|Mentioned|Table 1|||||||||
26448|Callytharra Formation|40617|6|Mentioned|Fig.1|||||||||
26448|Callytharra Formation|41044|6|Mentioned|p128|||||||||
26448|Callytharra Formation|41049|6|Mentioned|p44|||||||||
26448|Callytharra Formation|41053|6|Mentioned|p97|||||||||
26448|Callytharra Formation|41071|6|Mentioned|p34|||||||||
26448|Callytharra Formation|41100|6|Mentioned|p271|||||||||
26448|Callytharra Formation|41271|3|Fully described|p76|||Formerly "C. Limestone Group" 1932, "C. Stage" 1932||||||
26448|Callytharra Formation|41315|6|Mentioned|p155|||||||||
26448|Callytharra Formation|41436|6|Mentioned|p42|||||||||
26448|Callytharra Formation|41438|4|Described|p103|||See also Fig.11||||||
26448|Callytharra Formation|41443|5|Briefly described|p163|||||||||
26448|Callytharra Formation|41514|6|Mentioned|p79|||||||||
26448|Callytharra Formation|41689|6|Mentioned|Table 1|||||||||
26448|Callytharra Formation|41809|6|Mentioned|p71|||||||||
26448|Callytharra Formation|41839|6|Mentioned|p20|||||||||
26448|Callytharra Formation|42017|6|Mentioned|p1|||||||||
26448|Callytharra Formation|42116|4|Described|p27|||See also Fig.1 P5||||||
26448|Callytharra Formation|42392|5|Briefly described|p113|||||||||
26448|Callytharra Formation|42462|6|Mentioned|p55|||||||||
26448|Callytharra Formation|42473|6|Mentioned|p66|||||||||
26448|Callytharra Formation|42540|5|Briefly described|p312|||Carnarvon Basin||||||
26448|Callytharra Formation|42547|5|Briefly described|p91|||||||||
26448|Callytharra Formation|42994|5|Briefly described|p35|||||||||
26448|Callytharra Formation|43015|5|Briefly described|Table 1,p319|||||||||
26448|Callytharra Formation|43018|6|Mentioned|p390|||||||||
26448|Callytharra Formation|43050|6|Mentioned|p6|||One of the locations for the fossil Earlandia condoni Crespin 1958. Geological Province: Carnarvon Basin.||||||28-OCT-09
26448|Callytharra Formation|43255|5|Briefly described|map legend||Sakmarian|||||||
26448|Callytharra Formation|43256|5|Briefly described|5-22||Permian|||||||
26448|Callytharra Formation|43474|14|Not recorded|p71|||||||||
26448|Callytharra Formation|43737|6|Mentioned|p3||Sakmarian|||||||
26448|Callytharra Formation|43835|5|Briefly described|Map Legend||Sakmarian|||||||
26448|Callytharra Formation|43879|14|Not recorded|p254||Permian|Carnarvon Basin||||||
26448|Callytharra Formation|44040|14|Not recorded|p43,44|||||||||
26448|Callytharra Formation|44217|14|Not recorded|p5|||Fig 3.||||||
26448|Callytharra Formation|44219|14|Not recorded|p31||Sakmarian|||||||
26448|Callytharra Formation|44344|14|Not recorded|7-10||Artinskian|Early Artinskian; o/lies Lyons Group. (G50-1). opp.5; map.||||||
26448|Callytharra Formation|44345|14|Not recorded|map legend||Artinskian|||||||
26448|Callytharra Formation|44532|4|Described|p.3,4,6, map|||(G50-5).||||||
26448|Callytharra Formation|44533|5|Briefly described|map legend||Artinskian|Artinskian.||||||
26448|Callytharra Formation|44537|14|Not recorded|map legend||Artinskian|||||||
26448|Callytharra Formation|44657|14|Not recorded|p.5,7,8,16|||||||||
26448|Callytharra Formation|44994|6|Mentioned|p13|||||||||
26448|Callytharra Formation|45001|14|Not recorded|p7|Artinskian|Sakmarian|||||||
26448|Callytharra Formation|45015|5|Briefly described|p7, p8, map legend|Artinskian|Sakmarian|Limestone unit first described by Maitland (1901). Geological Province: Carnarvon Basin.||||||28-OCT-09
26448|Callytharra Formation|45016|2|Defined|p64-69, 71-75||Artinskian|Tb. at back, p.12,14,16,18,19,22-25,27-28,44,46,47, Fig.56,49-51,53-64,77-81,83-94,98-101,103-5,107-12,115,119,121,122,132,136,140,143,148,161,163,Figs. 59,65. (F49-12,16,F50-9,13,G50-1,2,,5,6,9,10,G49-4).||||||
26448|Callytharra Formation|45031|14|Not recorded|p22,37,40,42,54,57-8||Permian|p60,63||||||
26448|Callytharra Formation|46849|6|Mentioned|Fig. 6|||See also P199||||||
26448|Callytharra Formation|47041|6|Mentioned|Fig.2|||||||||
26448|Callytharra Formation|48573|14|Not recorded|p.12.|||(E51-7/Alexander Creek)||||||
26448|Callytharra Formation|48610|4|Described|p4, Pl.1,2|||(F50-13).||||||
26448|Callytharra Formation|48628|14|Not recorded|Fig.5|||||||||
26448|Callytharra Formation|48831|14|Not recorded|p.35|||On many pages. p.7,9,12,16-19,21-24,32,33,35,39-41,53,55-59,63-65,68-70.||||||
26448|Callytharra Formation|48848|14|Not recorded|p.54|||On many pages. p.13,23,33,39,47,49-51,54,56-7,61,64,66-7,69-70,72-6,79-80,83.||||||
26448|Callytharra Formation|48885|14|Not recorded|p.1,2,7-9,11,13,17||Early Permian|Lower Permian (Sakmarian-Artinskian). (G/50-6). Pls.1,2.||||||
26448|Callytharra Formation|48925|6|Mentioned|p12|||Permian age. Fauna P26 etc.||||||
26448|Callytharra Formation|49644|5|Briefly described|Table|||||||||
26448|Callytharra Formation|50085|5|Briefly described|p19 Fig. 10|Permian|Permian|Geological Province: Southern Carnarvon Basin.||||||
26448|Callytharra Formation|60295|5|Briefly described|p132|Artinskian|Sakmarian|Geological Province: Carnarvon Basin||||||
26448|Callytharra Formation|60296|5|Briefly described|p156 Fig.1|Sakmarian|Sakmarian|Correlated with Cranky Corner Sandstone, Allandale Formation, lower Pebbley Beach Formation, Golden Valley Group and Bundella Formation. Geological Province: Carnarvon Basin.||||||
26448|Callytharra Formation|60331|5|Briefly described|p33 Fig.2|Artinskian|Sakmarian|Geological Province: Southern Carnarvon Basin.||||||30-JUN-05
26448|Callytharra Formation|60386|5|Briefly described|p297, 309|Artinskian|Artinskian|Carnarvon Basin. Deltaic - nearshore - shelf.||||||
26448|Callytharra Formation|60725|5|Briefly described|p29 Fig.2, p30, p35 Fig.5, p36 Fig.6. |Early Permian|Early Permian|||||||
26448|Callytharra Formation|61023|5|Briefly described|p34 Fig. 14|Permian|Permian|Geological Province: Southern Carnarvon Basin.||||||11-APR-08
26448|Callytharra Formation|61958|5|Briefly described|Map sheet 1|Artinskian|Artinskian|||||||
26448|Callytharra Formation|64580|4|Described|map legend||Early Permian|Fossiliferous calcareous siltstone to calcisiltite; interbedded hard fossiliferous calcarenite.||||||09-DEC-08
26448|Callytharra Formation|64630|5|Briefly described|p31 Fig.2|Artinskian|Sakmarian|Province: Southern Carnarvon Basin. Underlies the Wooramel Group, overlies the Carrandibby Formation and undifferentiated Lyons Group. Palynology age: P. pseudoreticulata to M. trisina.||||||24-NOV-09
26448|Callytharra Formation|64972|6|Mentioned|p616 Fig. 3, p617 Fig. 5|Early Permian|Early Permian|||||||
26448|Callytharra Formation|64974|5|Briefly described|p143, p147 Fig. 5|Artinskian|Sakmarian|Includes Jimba Jimba Calcarenite. Geological Province: Carnarvon Basin.||||||24-JUN-09
26448|Callytharra Formation|66189|6|Mentioned|p454, p455 Fig.2|Sakmarian|Sakmarian|Overlies the glacial Lyons Group. Is overlain by Wooramel Group.||||||
26448|Callytharra Formation|66579|5|Briefly described|Map legend|Permian|Permian|Southern Carnarvon Basin.|||||Fossiliferous calcareous siltstone to calcisiltite; interbedded and fossiliferous calcarenite.|
26448|Callytharra Formation|66949|6|Mentioned|p22|||Carnarvon Basin.||||Corelated with Nura Nura Member (Poole Sandstone).||
26448|Callytharra Formation|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes dark grey very fossiliferous shale.|
26448|Callytharra Formation|67200|5|Briefly described|p7 fig 5, p47, p50, p55, app 2 p5|Sakmarian|Asselian |Thermal conductivity of 1.87 W/mK|||Includes Ballythanna Sandstone Member|Overlies Carrandibby Formation, overlain by Cordalia Formation|Interbedded siltstone and limestone with inverterbrate macrofossils. Fossiliferous Shale.|
26448|Callytharra Formation|67354|5|Briefly described|p106.|||Carnarvon Basin. Apparent correlative of marine beds in Ditji Formation, Bonaparte Basin. Contains conodont-bearing limestones.||||||
26448|Callytharra Formation|67373|5|Briefly described|Map legend.|Permian|Permian|Southern Carnarvon Basin.|||||Fossiliferous, calcareous siltstone to calcisiltite; interbedded hard fossiliferous calcarenite.|
26448|Callytharra Formation|67977|5|Briefly described|p479-483, p485, p487, p489, p491, p492|Artinskian|Sakmarian|Carbonate rich depositional environment. Locally sand-prone facies (Winnemia Sandstone Member and Ballythanna Sandstone Member) record fluvio-deltaic incursions into the basin (Mory and Backhouse, 1997). Geol. Prov: Southern Carnarvon Basin. Detailed facies associations included in paper. Lower Permian (Sterlitamakian - Aktastinian).|||Winnemia Sandstone Member and Ballythanna Sandstone Member|conformably overlies Lyons Group; is conformably overlain by Wooramel Group; is overlain by Cordalia Formation and Keogh Formation|limestone, variably fossiliferous siltstone, argillaceous carbonates|18-SEP-14
26448|Callytharra Formation|69011|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin.||||Overlain by the Moogooloo Sandstone (Wooramel Group). Underlain by the Lyons Group.|Comprises fossiliferous, calcareous siltstone to calcisiltite; interbedded, hard, fossiliferous calcarenite.|28-APR-14
26448|Callytharra Formation|69028|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin.|||||Fossiliferous, calcareous siltstone to calcisiltite; interbedded, hard fossiliferous calcarenite.|06-MAY-14
26448|Callytharra Formation|69029|6|Mentioned|p326,328|Sakmarian|Sakmarian|Of onshore Carnarvon Basin.||||Overlain by Wooramel Group. Underlain by Lyons Group.||
26448|Callytharra Formation|69166|5|Briefly described|geologyp_lut.csv|Sakmarian|Sakmarian||||||Fossiliferous, calcareous siltstone to calcisiltite; interbedded, hard fossiliferous calcarenite|
26448|Callytharra Formation|69182|6|Mentioned|Ch2 p3, Ch3 p3, Ch3 p8|Permian|Permian|Perth Basin. Incorrectly referred to (and misspelt as) the Callythara Group in Ch3 p45. Seals the underlying Lyons Group. See also Ch3 p10-p11, Ch3 p13, Ch3 p19-p20, Ch3 p23, Ch3 p29, Ch3 p35, Ch3 p55, Ch3 p67-p69, Ch3 p71, Ch3 p73. ||||Overlies the Lyons Group.||
26448|Callytharra Formation|69547|4|Described|p180-182,188,193-200, p202|Artinskian|Sakmarian|Southern Carnarvon Basin. Type section: 113 km SE of the Jimba Jimba Anticline. [type section also described from Dead Man's Gully, is this the same location?]. Deposited in much cooler water than the west Australian late Sakmarian-early Artinskian deposits.||Unit of Wooramel Group.|Includes Jimba Jimba Calcarenite Member and Winnamea Sandstone Member.|Overlain by Nunnery Sandstone. Underlain by Carrandibby Formation/Lyons Group.|Limestone interbedded with mudstone or fine-grained sandstone.|09-JUL-19
26448|Callytharra Formation|69583|5|Briefly described|p130, p134 Fig.3, Plates 3, 4|Permian|Permian|Southern Carnarvon Basin. Seismic interpretation.|||||Fossiliferous, calcareous siltstone to calcisiltite; interbedded, hard fossiliferous calcarenite.|
26448|Callytharra Formation|70138|5|Briefly described|Map legend.|Permian|Permian|Southern Carnarvon Basin.|||||Fossiliferous, calcareous siltstone to calcisiltite; interbedded, hard, fossiliferous calcarenite.|
26448|Callytharra Formation|70774|5|Briefly described|p5 fig 3, p40|Artinskian|Sakmarian|Southern Carnarvon Basin. Includes Ballythanna [Sandstone Member].||||Overlies the Carrandibby Formation and the Lyons Group. Overlain by the Cordalia Formation (Wooramel Group). Equivalent to the Nura Nura Member.||06-FEB-20
26448|Callytharra Formation|70795|4|Described|100k_geologyp_lut.csv|Sakmarian|Sakmarian|Also 100k_interpgeop_lut.csv|295-290 Ma||||Fossiliferous, calcareous siltstone to calcisiltite; interbedded, hard, fossiliferous calcarenite.|
26448|Callytharra Formation|71146|5|Briefly described|p6|Sakmarian|Sakmarian|Southern Carnarvon Basin.||||Overlies the Lyons Group. Overlain by the Wooramel Group.|Mudstone and carbonate.|
26448|Callytharra Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, calcarenite|
26448|Callytharra Formation|72034|5|Briefly described|500k_interpgeop16_lut|Sakmarian|Sakmarian|Glacigene rocks, Southern Carnarvon Basin.  Age from biostratigraphy.|||||Fossiliferous, calcareous siltstone to calcisiltite; interbedded, hard, fossiliferous calcarenite.|
26448|Callytharra Formation|72505|5|Briefly described|p890|Artinskian|Sakmarian|Southern Carnarvon Basin. Correlated with the P.Confluens and Microbaculaspora trisina zones.||||Overlies the Lyons Group. Overlain by the Wooramel Group.||
26448|Callytharra Formation|72910|4|Described|p1, 4,5, p7-26, p30-34, p36, 39, 40.|Artinskian|Sakmarian|Thickness 60-265m. Identified in Byro Sub-basin. Type section: Wooramel River, south end of Carrandibby Range, 25d30m30sS, 115d30m00sE. See also p41-42. Brachiopods in the upper part of this formation (previously assigned to Jimba Jimba Calcarenite Member) provide a minimum Artinskian age. Difficult to distinguish from Carrandibby Formation in drill core. Includes Barrabiddy Formation of previous authors. The upper part of this unit is laterally equivalent to the Cordalia Formation.|||Ballythanna Sandstone Member Winnemia Sandstone Member.|Overlies Lyons Gp. conformably, High Cliff Ss., Irwin River Coal Measures. Underlies Wooramel Gp. conformably, Keogh Fm., Cordalia Fm. Laterally equiv. to Holmwood Sh.|Fossiliferous grey-green calcareous siltstone and claystone with hard fossiliferous calcarenite; minor sandstone.|18-FEB-21
26448|Callytharra Formation|73117|6|Mentioned|p15, p22, p111|Artinskian|Artinskian|Southern Carnarvon Basin.|||Ballythanna Sandstone Member|Underlain by Lyons Group. Overlain by Wooramel Group.||
26448|Callytharra Formation|73623|5|Briefly described|p4, 16|Cisuralian|Sakmarian|Merlinleigh Basin. Maximum age from ammonoids in the basal part of the unit. Various biota discussed.|||Winnemia, Ballythanna, Sandstone Members.|Overlies Lyons Group. Is overlain by Wooramel Group. Correlative of Holmwood Shale.||
26449|Calyie Formation|22897|6|Mentioned|102|||Geol province Bangemall Basin||||||
26449|Calyie Formation|22905|5|Briefly described|p52 Fig. 2, p53 Table 1|Mesoproterozoic|Mesoproterozoic|Replaces the Calyie and Mount Vernon Sandstones.  Of the Collier Subgroup. Sandstone and siltstone. Overlying unit: Ilgarari Formation; underlying unit: Backdoor Formation. Max.thickness: 130m. See also p54.||||||24-JAN-06
26449|Calyie Formation|23156|4|Described|p9|Mesoproterozoic|Mesoproterozoic|Previously called the Calyie Sandstone, this unit has been reduced in area and is restricted to the sothwestern and northwestern corners of BULLEN||||||
26449|Calyie Formation|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Bangemall Group. Geological Province: Bangemall Basin.||||||
26449|Calyie Formation|23749|4|Described|p15|Proterozoic|Proterozoic|Of Bangemall Group. Geological Province: Bangemall Basin.||||||
26449|Calyie Formation|23750|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Bangemall Group. Geological Province: Bangemall Basin.||||||
26449|Calyie Formation|24115|4|Described|p4 Fig.2|Mesoproterozoic|Mesoproterozoic|Of the Collier Group. Maximum Thickness: 130m. Overlies the Backdoor Formation. Overlain by the Ilgarari Formation. Geological Province: Collier Basin.||||||
26449|Calyie Formation|24183|2|Defined|p4 Fig.3, p21|Stenian|Ectasian|Geological Province: Bangemall Basin. Max. Thickness: 1220m. Overlies the Backdoor Formation. Overlain by the Ilgarari Formation. Age: c.1300-1070 Ma.||||||
26449|Calyie Formation|24544|4|Described|p44 FIg.32|Mesoproterozoic|Mesoproterozoic|Of Collier Group. Superseded Mount Vernon Sandstone. Overlies Backdoor Formation. Overlain by Ilgarari Formation.||||||
26449|Calyie Formation|37214|4|Described|p9|||||||||22-DEC-09
26449|Calyie Formation|40355|5|Briefly described|p12|||||||||
26449|Calyie Formation|40989|6|Mentioned|Fig.1|||||||||
26449|Calyie Formation|41667|5|Briefly described|p36|||||||||
26449|Calyie Formation|42013|5|Briefly described|Map Legend|Proterozoic||||||||
26449|Calyie Formation|43209|5|Briefly described|map legend||Mesoproterozoic|Of Collier Subgroup.||||||
26449|Calyie Formation|43756|6|Mentioned|p533||Proterozoic|||||||
26449|Calyie Formation|50010|5|Briefly described|p58|||Overlies: Backdoor Formation.||||||
26449|Calyie Formation|50225|4|Described|p387 Fig. 2, p396|||Of the Collier Group (Bangemall Supergroup). Supersedes Mount Vernon Sandstone (of the former Bangemall Group). Contact with Backdoor Formation below is gradational.  Max. thickness: 200m.||||||07-FEB-11
26449|Calyie Formation|60301|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Collier Group (Bangemall Supergroup). Geological Province: Collier Basin. Quartz sandstone, siltstone, mudstone, conglomerate, and dolostone.||||||17-AUG-04
26449|Calyie Formation|60535|5|Briefly described|p556 Fig.1|Mesoproterozoic|Mesoproterozoic|Of the Collier Group (Bangemall Supergroup).||||||
26449|Calyie Formation|63866|5|Briefly described|p162|||||Collier Group||||
26449|Calyie Formation|63869|4|Described|p39, p40, p41-42, Plate 1|Mesoproterozoic|Mesoproterozoic|Formerly Calyie Sandstone (Brakel and Muhling, 1976; revised by Cooper et al., 1998). Renamed Calyie Formation (Martin et al., 1999) to incorporate the former Mount Vernon Sandstone and to reflect lithological variation. Cliff-forming unit. 190 m thick. Ages inferred from detrital zircons and dolerite sills.|< c.1400 - c.1070 Ma.|Unit in Collier Group.||Gradationally overlies Backdoor Formation. Is overlain conformably by Ilgarari Formation.|Basal thick-bedded, coarse- to very coarse-grained sandstone interbedded with siltstone; then medium- to very thick-bedded, medium- to coarse-grained quartz sandstone, massive to cross-stratified, interbedded with minor planar-laminated siltstone.|
26449|Calyie Formation|64580|6|Mentioned|map legend||Mesoproterozoic|Of Collier Group. Part of depositional package 5 (Backdoor and Calyie Formations).||||||15-DEC-08
26449|Calyie Formation|64728|5|Briefly described|p95, pp106-107.|Mesoproterozoic|Mesoproterozoic|Shallow marine and fluvial facies.||Unit in middle Collier Group.||Overlies Backdoor Formation. Is overlain by Ilgarari Formation.|Medium-grained, massive to trough cross-stratified quartz sandstone.|
26449|Calyie Formation|64772|5|Briefly described|p13, Plate 1  legend|Mesoproterozoic|Mesoproterozoic|Of the Collier Group. Geological province: Collier Basin. Quartz sandstone and minor siltstone, mudstone, conglomerate and dolostone.||||||01-MAR-11
26449|Calyie Formation|65830|4|Described|p7, p8-11, p16, p19; Plates 1,2|Stenian|Calymmian|190m thick. Predominantly deposited in a shallow-marine to fluvial depositional environment. Characterised by rapid facies changes. Uppermost unit of the Collier Group.||Of the Collier Group||Gradationally overlies the Backdoor Formation. Overlain by the Ilgarari Formation.|Consists mainly of very thick to medium-bedded, medium- to coarse-grained quartz sandstone that is typically massive to trough cross-stratified, and is interbedded with minor planar-laminated siltstone.|
26449|Calyie Formation|65896|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Unit in upper Collier Group, Bangemall Supergroup. Fine- to medium-grained quartz sandstone.||||||
26449|Calyie Formation|66104|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Unit in Collier Group. Quartz sandstone, siltstone, mudstone, conglomerate and dolostone. Includes two mapped but unnamed units; one of thin- to thick-bedded sandstone and siltstone, the other of siltstone and minor sandstone.||||||05-APR-13
26449|Calyie Formation|66107|5|Briefly described|p4 Fig.1 |Mesoproterozoic|Mesoproterozoic|||Of the Collier Group||||
26449|Calyie Formation|66112|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Unit in Collier Group. Quartz sandstone, siltstone, mudstone, conglomerate, and dolostone.||||||
26449|Calyie Formation|66241|5|Briefly described|pp1-4, p9. |Mesoproterozoic|Mesoproterozoic|Submarine fan deposits.||Unit in Collier Group.||Overlies Backdoor Formation. Is overlain by Ilgarari Formation.|Thick-bedded fine- to medium-grained quartz sandstone and siltstone.|
26449|Calyie Formation|67136|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin.||Unit in Collier Group.||Overlies Backdoor Formation. Is overlain by Ilgarari Formation.|Quartz sandstone, siltstone, mudstone, conglomerate and dolostone.|14-NOV-11
26449|Calyie Formation|67374|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin.||Unit in Collier Group.|||Quartz sandstone, siltstone, mudstone, conglomerate and dolostone.|
26449|Calyie Formation|68285|5|Briefly described|Map Legend|Stenian|Calymmian|Collier Basin.||Of the Collier Group.|One informal unnamed member shown.|Overlain by the Ilgarari Formation. Underlain by the Backdoor Formation.|Quartz sandstone, siltstone, mudstone, conglomerate, and dolostone; siltstone, mudstone, and thin- to thick-bedded quartz sandstone.|
26449|Calyie Formation|68286|5|Briefly described|Map Legend|Stenian|Calymmian|Collier Basin.||Of the Collier Group||Overlain by the Ilgarari Formation. Underlain by the Backdoor Formation.|Thin- to thick-bedded quartz sandstone, siltstone, mudstone, conglomerate, and dolostone.|
26449|Calyie Formation|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic|Described together with backdoor Formation as: siltstone, mudstone, sandstone; minor dolostone, chert, and conglomerate.||Collier Group||||
26449|Calyie Formation|69003|5|Briefly described|p34, p53|Mesoproterozoic|Mesoproterozoic|Collier Basin, Capricorn Orogen.||Collier Group.||Overlies backdoor Formation. Is overlain by Ilgarari Formation.|Fluvial-deltaic siliciclastic sedimentary rocks.|
26449|Calyie Formation|69010|5|Briefly described|Map Legend|Stenian|Calymmian|Collier Basin. Two facies are mapped separately: siltstone and minor sandstone; and thin- to thick-bedded sandstone and siltstone.|1460-1070 Ma|Of the Collier Group.|||Comprises quartz sandstone, siltstone, mudstone, conglomerate and dolostone.|24-APR-14
26449|Calyie Formation|69027|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Collier Basin.||Of the Collier Group.||Underlain by the Backdoor Formation. Overlain by the Ilgarari Formation.|Quartz sandstone, siltstone, mudstone, conglomerate, and dolostone.|05-MAY-14
26449|Calyie Formation|69028|5|Briefly described|Map Legend|Stenian|Stenian|Collier Basin. Mapped with Backdoor Formation as a single unit.||Of the Collier Group.|||Siltstone, mudstone and sandstone; minor dolostone, chert and conglomerate.|06-MAY-14
26449|Calyie Formation|69091|5|Briefly described|p202|||Collier Basin. Thickness: ~200 m (Cutten et al., 2011)|||||Interbedded medium- to coarse-grained sandstone and siltstone.|
26449|Calyie Formation|69166|4|Described|geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|||Collier Group||Overlies Backdoor Formation|Siltstone and minor sandstone, thin-thickly bedded sandstone, quartz sandstone mudstone, conglomerate and dolostone.|
26449|Calyie Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|||Part of Collier Group Depositional package 5.||Unit of Collier Group.||||
26449|Calyie Formation|69596|6|Mentioned|p12 Fig.7|||Collier Basin.||Collier Group.||||
26449|Calyie Formation|70132|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Collier Basin. Three facies associations are mapped separately.||Collier Group.||Overlies Backdoor Formation. Is overlain by Ilgarari Formation.|Quartz sandstone, subordinate siltstone, minor conglomerate. Thin- to thick-bedded sandstone and siltstone; siltstone and minor sandstone; siltstone and thin- to thick-bedded quartz sandstone.|
26449|Calyie Formation|70136|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Collier Basin. Two facies associations are mapped separately.||Collier Group.|||Quartz sandstone, siltstone, mudstone, conglomerate and dolostone. Siltstone and minor sandstone; thin- to thick-bedded sandstone and siltstone.|
26449|Calyie Formation|70767|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin.|<1171 Ma.|Collier Group.||Overlies Backdoor Formation. Is overlain by Ilgarari Formation. Is intruded by Kulkatharra Dolerite.|Quartz sandstone and subordinate siltstone; minor conglomerate. Two sub-units are mapped separately: siltstone and minor sandstone; siltstone and thin- to thick-bedded quartz sandstone.|
26449|Calyie Formation|70768|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin.|<1171 Ma.|Collier Group.||Overlies Backdoor Formation. Is overlain by Ilgarari Formation. Is intruded by Kulkatharra Dolerite. Faulted against Glass Spring Formation (Salvation Group).|Quartz sandstone and subordinate siltstone; minor conglomerate. Two sub-units are mapped separately: siltstone and minor sandstone; siltstone and thin- to thick-bedded quartz sandstone.|
26449|Calyie Formation|70795|5|Briefly described|100k_geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Also 100k_interpgeop_lut.csv, West Australian Craton, Collier Basin|1171-1070 Ma|Collier Group||Overlies Backdoor Formation|Quartz sandstone and subordinate siltstone; minor conglomerate.|
26449|Calyie Formation|70814|4|Described|p5, p15-p17, p20, p22, p25-p29, p37|||Collier Basin. Interpreted to have been deposited during delta progradation. Outcrop characteristics discussed. This unit is up to 1800m thick and interpreted to have been deposited in a delta-front or delta-top environment.||Collier Group||Conformably overlies the Backdoor Formation. Conformably overlain by the Ilgarari Formation.|Thin to very thickly-bedded quartz sandstone and subordinate siltstone with minor conglomerate.|
26449|Calyie Formation|71158|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin. Two facies associations are mapped separately: siltstone and thin- to thick-bedded quartz sandstone; and thin- to thick-bedded sandstone and siltstone.||Collier Group.|||Quartz sandstone and subordinate siltstone; minor conglomerate.|
26449|Calyie Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Collier Group.|||Recrystallised fine to coarse sandstone, in places glauconitic, with lesser interbedded siltstone, granule to pebble conglomerate, shale, mudstone, dolostone, pebbly sandstone, minor chert and dolostone|
26449|Calyie Formation|71269|5|Briefly described|1m_geologyp12_lut.csv|||Geological province: Capricorn Orogen; West Australian Craton. ||Unit of Collier Group.|||Recrystallised fine to coarse sandstone, in places glauconitic, with lesser interbedded siltstone, granule to pebble conglomerate, shale, mudstone, dolostone, pebbly sandstone, minor chert and dolostone|
26449|Calyie Formation|72259|6|Mentioned|p3|||||Collier Group||||
26449|Calyie Formation|72705|5|Briefly described|p3|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||Collier Group.||Overlies Backdoor Formation. Is overlain by Ilgarari Formation.||
26449|Calyie Formation|73442|5|Briefly described|p20|||||||Intruded by Kulkatharra Dolerite|Includes dolomite, siltstone and fine-grained sandstone.|
23457|Calypso Formation|12491|5|Briefly described|p453.|Middle Jurassic|Early Jurassic|Exmouth Sub-basin. Rifting initiated during Pliensbachian forming a major depocentre.||||Overlies Athol Formation. Is overlain by Dingo Formation|Monotonous sequence of silty shales deposited in low-energy, marine setting with restricted circulation.|
23457|Calypso Formation|12498|6|Mentioned|p517 Fig.3. |Middle Jurassic|Middle Jurassic|||||Overlies Legendre Formation. Is overlain by Dingo Claystone.||
23457|Calypso Formation|42615|3|Fully described|p32|Oxfordian early||Reserved.||||||
23457|Calypso Formation|60379|5|Briefly described|p125, p126 fig 3, p128, p129-130|Oxfordian|Callovian|Dampier sub-basin, Carnarvon Basin. Marine claystones. Seal for Legendre Formation hydrocarbon play.||||||
23457|Calypso Formation|60384|6|Mentioned|p244, p243 Fig 2b|Middle Jurassic|Late Triassic|Exmouth Sub-basin, Northern Carnarvon Basin.||||||
23457|Calypso Formation|60386|6|Mentioned|p300, 302|Late Jurassic|Middle Jurassic|Northern Carnarvon Basin/Browse Basin. Proximal shelf.||||||
23457|Calypso Formation|62837|5|Briefly described|Stratigraphic columns|Bathonian|Bathonian|Age: ~164-160Ma. Geological Province:  Dampier Sub-basin, Rankin Platform and Beagle Sub-basin.||||||01-MAR-10
23457|Calypso Formation|63950|5|Briefly described|p336 Fig. 4|Late Jurassic|Late Jurassic|Overlies Legendre and Learmonth Formations; underlies Dingo Claystone. Geological Province: northern Carnarvon Basin.||||||27-MAY-08
23457|Calypso Formation|64978|6|Mentioned|p528 Fig.2.|Middle Jurassic|Middle Jurassic|Includes Callovian sandstones forming part of Perseus hydrocarbon reservoir.||||||
23457|Calypso Formation|66126|6|Mentioned|p206|Middle Jurassic|Middle Jurassic|Carnarvon Basin.||||||
23457|Calypso Formation|67368|6|Mentioned|p209 Fig.4.|Callovian|Callovian|||||Overlies Legendre Formation. Is overlain by Eliassen Formation.||
23457|Calypso Formation|68135|5|Briefly described|p51 fig 2a|Middle Jurassic|Middle Jurassic|Northern Carnarvon Basin.|||Emma Member.|Overlies Athol and Legendre Formations.||14-SEP-17
23457|Calypso Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Northern Carnarvon Basin.||||Overlies Learmonth Formation, Murat Siltstone, Depuch Formation. Is overlain by Eliassen Formation.||
23457|Calypso Formation|69692|6|Mentioned|p4|Late Jurassic|Late Jurassic|Northern Carnarvon Basin.||||Overlies Athol Formation. Is overlain by Dingo Formation.||
23457|Calypso Formation|70066|5|Briefly described|Dampier: Fig.2; p2. Exmouth: Fig.2|Oxfordian|Callovian|See also Regional: Fig.6; p5. Northern Carnarvon Basin. Represents initial syn-rift deposition in the Barrow and Dampier Sub-basins. Fluvio-deltaic to marine sediments are potential reservoirs.||||Overlies Legendre Formation. Is overlain by Dingo Claystone or Eliassen Formation.|Transgressive claystone and sandstone.|
23457|Calypso Formation|73564|6|Mentioned|p1225|Jurassic|Jurassic|Exmouth Sub-basin.||||Overlies Murat Siltstone. Is overlain by Barrow Group.||
31466|Calytrix Formation|23523|4|Described|p995|Early Permian|Early Permian|Of Grant Group. See also p997.  Geological Province: Canning Basin.||||||
31466|Calytrix Formation|43823|4|Described|p753|||||||||
31466|Calytrix Formation|60295|5|Briefly described|p130|||Geological Province: Carnarvon Basin||||||
31466|Calytrix Formation|64580|6|Mentioned|map legend|||Of Grant Group.||||||24-NOV-08
31466|Calytrix Formation|64630|5|Briefly described|p31 Fig.2, p35|Sakmarian|Sakmarian|N.B. Tentative ages, awaiting further palynology work. Province: subsurface Barbwire Terrace area, Canning Basin.  Part of the Grant Group, underlies the Clianthus Formation, overlies the Hoya Formation. Palynology age: P. confluens.||||||19-OCT-09
31466|Calytrix Formation|64643|5|Briefly described|p8|Sakmarian|Sakmarian|Of Grant Group across the Barbwire Terrace.||||||24-NOV-08
31466|Calytrix Formation|64971|5|Briefly described|p684, p685 Fig. 2|Early Permian|Early Permian|Of Grant Group. Geological Province: Canning Basin.||||||09-FEB-10
31466|Calytrix Formation|66949|4|Described|p58 Appx.3, p10, p13-14, p18-20; p46-48,|Sakmarian|Sakmarian|See also 51-54 Appx.2, p60-65 Appx.4, p66-78,80-84,88,90-94 Appx.5; Plates 8-10,12. Type section in Pratia 1 detailed. Age from palynology. Up to 120m thick; shallow marine to lagoonal deposits. Little if any glacial influence in type area (Barbwire Terrace). Available core and Formation picks detailed.||Unit in Grant Group.||Conformably overlies Hoya Formation. Is overlain conformably by Clianthus Formation.|Siltstone, claystone, fine-grained sandstone, thin basal limestone.|30-OCT-15
31466|Calytrix Formation|67354|5|Briefly described|p93, p106, p108 Fig.39.|||Canning Basin. Calytrix-1 core contains marine shells but no clear marine palynomorphs. Discussed in relation to its equivalent, the Treachery Formation (Bonaparte Basin); absence of marine indicators as a function of sampling method, or development of long-lived brackish seas.||||Overlies Hoya Formation. Is overlain by Clianthus Formation.||30-OCT-15
31466|Calytrix Formation|68007|5|Briefly described|p9|Permian|Permian|||Grant Group.||Equivalent to Winifred Formation.||
31466|Calytrix Formation|68656|6|Mentioned|GEOL_LUT_CSV/500k_geologyp08_lut|||||Grant Group||||
31466|Calytrix Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Cisuralian|Pennsylvanian|||||||
31466|Calytrix Formation|69297|6|Mentioned|p337, p352|Sakmarian|Sakmarian|Broome Platform of the Canning Basin. ||Grant Group||Overlies the Hoya Formation. Overlain by the Clianthus Formation.||
31466|Calytrix Formation|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Grant Group.||||
31466|Calytrix Formation|69693|5|Briefly described|p3, 10|Sakmarian|Sakmarian|Barbwire Terrace, Canning Basin. See also reference to Calytrix formation (p4).||Grant Group||Overlies Hoya Formation. Is overlain by Clianthus Formation. Equivalent to Winifred Formation.|Mudstone.|
31466|Calytrix Formation|70774|5|Briefly described|p5 fig 3|Sakmarian|Sakmarian|Canning Basin.||Grant Group||Overlies the Hoya Formation. Overlain by the Clianthus Formation.||
31466|Calytrix Formation|72496|5|Briefly described|p217-220, p222, p230-231|Sakmarian|Sakmarian|Canning Basin, Barbwire Terrace. Interpreted by Redfern (1990) to have been deposited in a shallow marine to lacustrine environment with some evidence of glacial influence.||Grant Group||Equivalent to the Winifred Formation. Overlies the Hoya Formation. Overlain by the Clianthus Formation.||18-MAR-20
31466|Calytrix Formation|72497|5|Briefly described|p4.|Permian|Permian|After Redfern and Millward, 1994. Recognised in subsurface Barbwire Terrace area. Implied to be part equivalent to Carolyn Formation.||upper Grant Group||Shown as overlying Hoya Formation and underlying Clianthus Formation.||
31466|Calytrix Formation|73117|4|Described|p: 15, 22-26, 28, 32, 39, 111-113, 117|Asselian|Asselian|Name proposed by Redfern (1991) as an alternative subdivision of the Grant Group to that of Of Crowe and Towner (1975). Name derived from a well at the south-eastern end of the Barbwire Terrace. This scheme for constituents of the Grant Group has been applied inconsistently across the Barbwire Terrace. Proposed lectostratotype section from Pratia 1 well (Apak and Backhouse, 1999). Includes the P. confluens Zone. Mentioned as a potential top seal for hydrocarbon reservoirs.||Grant Group||Underlain[?] by Hoya Formation. Overlain[?] by Clianthus Formation.|Includes fossiliferous mudstone-limestone.|
72569|Calyx Corner beds|62735|5|Briefly described|p982, p984|Famennian|Frasnian|Informally named horizon within the Virgin Hills Formation in the McWhae Ridge area.  Geological Province: Canning Basin.||||||
23459|Camberathunun Formation|42533|3|Fully described|p67|||Name reserved.||||||
23459|Camberathunun Formation|44149|5|Briefly described|p35 fig 2-30, p38-40|Archean|Archean|Of Murchison Province||Yalgoo Subgroup||Overlies Wadgingarra Basalt.|Sheared and weathered felsic volcanic rocks; intensely deformed and altered, banded quartz-oligoclase-hornblende-chlorite rocks with fragmental textures; andesitic in composition, probably pyroclastic in origin.|
23459|Camberathunun Formation|65268|6|Mentioned|p6 fig 4||||||||Mostly felsic volcanic rocks.|
80952|Cambrian - Ordovician sedimentary rocks 80952|72034|5|Briefly described|500k_interpgeop16_lut|Early Ordovician|Series 2|Ord Basin. Unnamed unit. Age inferred.|||||Sandstone, siltstone, limestone.|
80996|Cambrian - Ordovician sedimentary siliciclastic units 80996|72034|5|Briefly described|500k_interpgeop16_lut|Ordovician|Cambrian|Amadeus Basin (Phase 2). Age inferred.|||||Siltstone and mudstone, sandstone, conglomerate, minor dolomite, shallow marine to fluvial.|
80122|Camel Bore Granodiorite|71212|4|Described|p75, p72, fig19, p90, p248|||Yilgarn Craton. Named for the Camel Bore. Crops out sporadically through sand and calcrete in an ovoid or wedge-shaped body in an overturned anticline. ||||Probably equivalent to the Lawlers Tonalite.|Strongly foliated and/or lineated grey, plagioclase-phyric tonalite to granodiorite.|26-SEP-17
80122|Camel Bore Granodiorite|73151|6|Mentioned|p4|||Yilgarn Craton.||||||
80122|Camel Bore Granodiorite|73596|6|Mentioned|p1167|Neoarchean|Mesoarchean|Southern Cross Domain. Appears descriptively as Camel Bore hornblende-granodiorite on p1167.|2802 +/- 3 Ma.|||||
33276|Camel Hills Metamorphics|22904|4|Described|p56|Paleoproterozoic|Paleoproterozoic|Age c. 1969 Ma||||||07-NOV-08
33276|Camel Hills Metamorphics|23485|4|Described|p16|Paleoproterozoic|Paleoproterozoic|Of Gascoyne Complex. Orginally included in the Morrisey Metamorphic Suite. Geological Province: Capricorn Orogen.||||||07-NOV-08
33276|Camel Hills Metamorphics|23486|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Complex.||||||07-NOV-08
33276|Camel Hills Metamorphics|23487|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Complex.||||||07-NOV-08
33276|Camel Hills Metamorphics|23525|5|Briefly described|p2 Fig. 1|Orosirian|Orosirian|Age: 2000-1960Ma.   Geological Province: Gascoyne Complex||||||
33276|Camel Hills Metamorphics|23780|5|Briefly described|p38|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
33276|Camel Hills Metamorphics|23781|5|Briefly described|p3|||Geological Province: Yilgarn Craton.||||||
33276|Camel Hills Metamorphics|24332|5|Briefly described|p135 Fig. 1|Paleoproterozoic|Paleoproterozoic|Metasedimentary rocks. Age: c.2000Ma. Within the Gascoyne Complex (Glenburgh Terrane).||||||07-NOV-08
33276|Camel Hills Metamorphics|24544|4|Described|p3|Paleoproterozoic|Paleoproterozoic|Metasedimentary and mafic and ultramafic meta-igneous rocks. Previously of Morrissey Metamorphic Suite.||||||07-NOV-08
33276|Camel Hills Metamorphics|50218|5|Briefly described|p240 Fig.2, p248|Orosirian|Orosirian|Includes the Quartpot Pelite and Petter Calc-silicate. Calc-silicate-gneiss and pelitic schists and gneisses. Age: <2025Ma. Geological Province: Errabiddy Shear Zone. See also p241 Fig. 3.||||||07-FEB-11
33276|Camel Hills Metamorphics|50219|5|Briefly described|p258 Fig. 1, p260 Fig. 2|Orosirian|Orosirian|Age: 2000-1960Ma.  Intruded by Moorarie and Bertibubba Supersuites.  Geological Province: Errabiddy Shear Zone.||||||07-FEB-11
33276|Camel Hills Metamorphics|50220|5|Briefly described|p280, p281 Fig.1|Orosirian|Orosirian|Metasedimentary rocks. Age: 2000 Ma. See also p292 Tb.2||||||
33276|Camel Hills Metamorphics|50226|5|Briefly described|p418|Paleoproterozoic|Paleoproterozoic|Of the Gascoyne Complex.||||||07-NOV-08
33276|Camel Hills Metamorphics|63869|5|Briefly described|p10, p17|||Errabiddy Shear Zone: the boundary between Gascoyne Complex and Yilgarn Craton. Protolith ages between c.2025 and c.1970 Ma (Occhipinti et al., 2001).|||||Deformed metasedimentary and mafic meta-igneous rocks.|
33276|Camel Hills Metamorphics|64580|4|Described|map legend||Paleoproterozoic|Pelite, calc-silicate rock, quartzite, metamorphosed banded iron formation and amphibolite.||||||15-DEC-08
33276|Camel Hills Metamorphics|65545|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Gascoyne Province. Includes Quartpot Pelite, Petter Calc-silicate and various unnamed metamorphosed units - BIF, amphibolite, quartzite etc. Age: c. 1985 Ma from age of veins intruding Quartpot Pelite. ||||||
33276|Camel Hills Metamorphics|65549|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Gascoyne Province. Includes Quartpot Pelite. Underlies Spring Camp Formation. Age <1985 Ma||||||
33276|Camel Hills Metamorphics|65830|6|Mentioned|p24||||||||Pelitic migmatites.|
33276|Camel Hills Metamorphics|65896|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Complex. Includes Petter Calc-silicate,  Quartpot Pelite and 3 unnamed units. <2025 Ma.||||||
33276|Camel Hills Metamorphics|66299|4|Described|pp3-5, pp95-104.|Paleoproterozoic|Paleoproterozoic|Volcanic arc-related medium- to high-grade metasedimentary rocks. Intruded by fault-bounded inliers of Warrigal Gneiss. Deformed by Capricorn Orogeny.|||Includes Quartpot Pelite and Petter Calc-silicate.|Associated with the intrusives of Dalgaringa Supersuite. Overlain by Mount James Subgroup. Faulted against several units including Dalgaringa Supersuite and Warrigal Gneiss.|Garnet-sillimanite-bearing pelitic and psammitic schists; metamorphosed banded iron-formation, amphibolite.|
33276|Camel Hills Metamorphics|66887|4|Described|p1, p3 Fig.2, p6, p22|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, southern Gascoyne Province. Arc-related metasedimentary rocks. Misspelt as Camel Hill Metamorphics on p5 Fig.4.|~2600-~1990 Ma estimated from Fig.4.||Petter Calc-silicate, Quartpot Pelite|In tectonic contact with Dalgaringa Supersuite.|High-grade metasedimentary rocks.|
33276|Camel Hills Metamorphics|66950|5|Briefly described|p7, p9 Fig.8, p10 Fig.9, p15|Orosirian|Neoarchean|Confined to the Errabiddy Shear Zone. Incorporates rocks reassigned from the now invalid Morrissey Metamorphics, including type areas from the original "Morrissey Metamorphic Suite" (Williams et al. 1978).|c. 2600-1955 Ma||Includes Quartpot Pelite and Petter Calc-silicate.||Comprises pelitic gneiss and schist; calc-silicate gneiss and schist with quartzite; and undivided amphibolite and metamorphosed banded iron-formation.|15-DEC-16
33276|Camel Hills Metamorphics|67843|4|Described|Throughout the article.|||Isolated, fault-bounded rocks of this unit occur in the Errabiddy Shear Zone, but nowhere else in the Capricorn Orogen. All units metamorphosed to amphibolite to granulite facies. Has strong migmatitic or gneissic fabric.|||Includes Quartpot Pelite and Petter Calc-silicate.||Calc-silicate gneiss, pelitic schists, gneisses.|
33276|Camel Hills Metamorphics|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic||||||pelite, calc-silicate rock, quartzite, metamorphosed banded iron formation and amphibolite|
33276|Camel Hills Metamorphics|69003|5|Briefly described|p4, p9-10|||Glenburgh Terrane. Capricorn Orogen. Fore-arc deposits to the Dalgaringa Arc.|2000-1995 Ma.||||Siliciclastic metasedimentary rocks.|
33276|Camel Hills Metamorphics|69028|5|Briefly described|Map Legend|Orosirian|Orosirian|Glenburgh Terrane, Gascoyne Province.|2000-1955 Ma||||Pelite, calc-silicate rock, quartzite, metamorphosed banded iron-formation and amphibolite.|06-MAY-14
33276|Camel Hills Metamorphics|69080|5|Briefly described|p684|||Gascoyne Province. Glenburgh Terrane.|||||Pelite, calc-silicate rock, quartzite, metamorphosed BIF and amphibolite.|
33276|Camel Hills Metamorphics|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic||||Includes Petter Calc-silicate, Quartpot Pelite||Amphibolite; fine grained hornblende--plagioclase--quartz--epidote--titanite rock|
33276|Camel Hills Metamorphics|69387|5|Briefly described|p3, p6, p13, p22-23, p25, p27-28, p66|Orosirian|Orosirian|Glenburgh Terrane, Gascoyne Province. SG and magnetic susceptibility values given. Gravity and magnetic modelling. Appears as Camel Hills Formation on p66.|2000-1975 Ma.||Quartpot Pelite, Petter Calc-silicate.||Iron-rich rocks. Has high lithological diversity.|
33276|Camel Hills Metamorphics|69583|5|Briefly described|p130-132, Plate 3|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Arc-related.|c.2000-1995 Ma.||||Pelite, calc-silicate rock, quartzite, metamorphosed BIF and amphibolite.|
33276|Camel Hills Metamorphics|69595|6|Mentioned|p19||||||Quartpot Pelite|||
33276|Camel Hills Metamorphics|70019|5|Briefly described|p94|Orosirian|Orosirian|Geological province: Gascoyne Province, Capricorn Orogen. Comprises Neoarchean to Paleoproterozoic basement rock assemblage of the Gascoyne Province. Package of medium- to high-grade metasedimentary rocks.|2000-1955 Ma|||||
33276|Camel Hills Metamorphics|70090|5|Briefly described|p453|||Geological province: Gascoyne Province.|||Includes Quartpot Pelite.|||
33276|Camel Hills Metamorphics|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 2_5m_interpgeop15_lut.csv, 100k_geologyl_lut.csv, 100k_interpgeop_lut.csv, 208325.1.pdf, West Australian Craton|2001-1955 Ma||||Amphibolite; fine grained hornblende-plagioclase-quartz-epidote-titanite rock. Pelite, calc-silicate rock, quartzite, metamorphosed banded iron formation and amphibolite.|
33276|Camel Hills Metamorphics|70796|4|Described|2_5m_interpgeop15_lut.csv|Paleoproterozoic|Paleoproterozoic|Of the Capricorn Orogen, Gascoyne Province, Glenburgh Terrane. Affected by the following events: Edmundian Orogeny (1026  954 Ma); Capricorn Orogeny (1817  1772 Ma); Glenburgh Orogeny D2 (1966  1947 Ma); Glenburgh Orogeny (2002  1947 Ma); Glenburgh Orogeny D1 (2002  1987 Ma). See also 500k_interpgeop14_lut.csv.|2001 +/ 26 Ma to 1955 +/7 ma (isotopic)||||Pelite, calcsilicate rock, quartzite, metamorphosed banded ironformation and amphibolite|
33276|Camel Hills Metamorphics|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|Southern Gascoyne Province. Time equivalent of the Tooloo Group. ||||Intruded by the Dalgaringa and Bertibubba Supersuites. May be equivalent to the Padbury Group.||
33276|Camel Hills Metamorphics|71000|6|Mentioned|p64-65, 79-80|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, southern Gascoyne Province, Capricorn Orogen.|2000-1955 Ma (deposition).|||Faulted against (in tectonic contact with) Moogie Metamorphics and Dalgaringa Supersuite.||
33276|Camel Hills Metamorphics|71269|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Gascoyne Province, Glenburgh Terrane, Capricorn Orogen, West Australian Craton. Events: Edmundian Orogeny (1026-954 Ma); Capricorn Orogeny (1817-1772 Ma); Glenburgh Orogeny D2 (1966-1947 Ma); Glenburgh Orogeny (2002-1947 Ma); Glenburgh Orogeny D1 (2002-1987 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv.|2002+\-26 Ma; 1955+\-7 Ma||Includes Petter Calc-silicate, Quartpot Pelite.||Pelite, calc-silicate rock, quartzite, metamorphosed banded iron-formation and amphibolite|
33276|Camel Hills Metamorphics|71484|5|Briefly described|p137|||Occurs west of the Padbury basin in the Errabiddy Shear Zone. Sedimentary protoliths possibly coeval with Tooloo Group sediments.|||Includes Quartpot Pelite.|||
33276|Camel Hills Metamorphics|71869|6|Mentioned|p4|||Emplaced during the Glenburgh Orogeny.||||||
33276|Camel Hills Metamorphics|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, Capricorn Orogen.|Max age 2001+/-26 Ma, min 1955 +/-7 Ma.||||Pelite, calc-silicate rock, quartzite, metamorphosed banded iron-formation and amphibolite.|
33276|Camel Hills Metamorphics|72259|6|Mentioned|App. Tb.B||||||||Includes pelitic migmatite and sandstone.|
33276|Camel Hills Metamorphics|73102|5|Briefly described|p3|||Gascoyne Province; Glenburgh Terrane.|||||Pelite, calc-silicaterock, quartzite, metamorphosed banded iron-formation and amphibolite.|
33276|Camel Hills Metamorphics|73214|5|Briefly described|p974 Fig.1|Palaeoproterozoic||Glenburgh Terrane.|||Quartpot Pelite, Petter Calc Silicate.|||
33276|Camel Hills Metamorphics|73442|5|Briefly described|p3|||Gascoyne Province, Glenburgh Terrane.|||||Pelite, calc-silicate rock, quartzite, metamorphosed banded iron-formation and amphibolite.|
79466|Camel Suite|71169|5|Briefly described|iv, vi, -p1, p54, p56-p60|Ectasian|Ectasian|Talbot, Connaughton and Tabletop Terranes; West Australian Craton. Pb/Pb dates of 1310 +/- 4 Ma (Nelson, 1996e), 1296 +/- 4 Ma (this study), 1291 +/- 10 Ma (Nelson, 1995b) and 1286 +/- 6 Ma (Bagas, 2004) are given. See also  p62, p68-p69, p71.|1310-1286 Ma||||Weakly deformed leucogranite and pegmatite.|
79466|Camel Suite|71795|4|Described|p31, p33-p34, p36, p38, p40|Ectasian|Ectasian|Rudall Province. Intrudes the Tabletop Terrane. Petrographic description and geochemsitry are briefly discussed, geodynamic implications are discussed in detail. See also p42-p44, p46-p49.|ca. 1310-1286 Ma||||Dominantly leucogranite.|
79466|Camel Suite|73168|5|Briefly described|p743, p760, p763|Ectasian|Ectasian|Rudall Province. Tabletop Domain.|1310-1286 Ma||||Leucogranites.|
26453|Campbell Sandstone|24160|6|Mentioned|p26, p27 Tb. 14|Proterozoic|Proterozoic|||Coomberdale Subgroup||||
26453|Campbell Sandstone|24410|5|Briefly described|p139|Proterozoic|Proterozoic|Of the Coomberdale Subgroup (Moora Group). See also p142 Tb. 60. ||||||
26453|Campbell Sandstone|36293|6|Mentioned|p76|||Refers Arriens & Lalor 1959 and Low 1975.||||||
26453|Campbell Sandstone|36872|3|Fully described|p74|||||||||
26453|Campbell Sandstone|37460|6|Mentioned|p178|||||||||
26453|Campbell Sandstone|40307|6|Mentioned|p64|||||||||
26453|Campbell Sandstone|40346|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26453|Campbell Sandstone|40347|6|Mentioned|p20|||||||||
26453|Campbell Sandstone|41957|6|Mentioned|p68|||||||||
72707|Campbell Well Granodiorite|64621|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite. Age: c.3313Ma. Biotite granodiorite, medium- to coarse-grained, foliated; metamorphosed.||||||07-NOV-08
72707|Campbell Well Granodiorite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Emu Pool Supersuite. c.3310 Ma. Biotite granodiorite; medium- to coarse-grained; foliated; weakly metamorphosed.||||||
72707|Campbell Well Granodiorite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Emu Pool Supersuite|||Biotite granodiorite; medium- to coarse-grained; foliated; weakly metamorphosed.|
72707|Campbell Well Granodiorite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3310 Ma (isotopic)|Unit of Emu Pool Supersuite.|||Biotite granodiorite; medium- to coarse-grained; foliated; weakly metamorphosed|
72707|Campbell Well Granodiorite|70733|6|Mentioned|p106||||3310 Ma.|||||
72707|Campbell Well Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||3310+/-3 Ma|Emu Pool Supersuite|||Biotite granodiorite; medium to coarse grained; foliated; weakly metamorphosed.|
38794|Campion Dolerite|23926|6|Mentioned|p33 Fig. 15|||Geological Province: Yilgarn Craton.||||||
38794|Campion Dolerite|23931|6|Mentioned|p200 Fig.2|||Geological Province: Yilgarn Craton.||||||
75800|Cane River supersequence|24607|5|Briefly described|p968|||Northwestern Ashburton Formation overlying June Hill Volcanics. Formerly considered coeval with Pingandy supersequence but now believed to be younger||||||
79346|Canegrass Granite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|3010-2600 Ma (inferred)||||Granite; typically poorly exposed and deeply weathered|
25830|Capalcarra Sandstone|24160|6|Mentioned|p27 Tb. 14|Proterozoic|Proterozoic|||Billeranga Subgroup||||
25830|Capalcarra Sandstone|24410|5|Briefly described|p143 Fig. 83|Proterozoic|Proterozoic|Of the Billeranga Subgroup (Moora Group). Unconformable over an Archaean basement. See also p142 Tb. 60.||||||24-NOV-09
25830|Capalcarra Sandstone|34705|6|Mentioned|p398|||||||||
25830|Capalcarra Sandstone|36293|2|Defined|p61|Proterozoic|Proterozoic|||||||
25830|Capalcarra Sandstone|36872|3|Fully described|p76|||||||||
25830|Capalcarra Sandstone|40347|6|Mentioned|p16|||||||||
25830|Capalcarra Sandstone|40348|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Middle or Late||||||
25830|Capalcarra Sandstone|40349|5|Briefly described|p13|||||||||
74631|Cape Boileau Calcarenite Member|64449|2|Defined|p75, p76, p79 Tb. 5, p87|Holocene|Holocene|Of Cable Beach Sand. Cemented beachrock composed of laminated, bedded, to low-angle cross-bedded, medium to fine to coarse calcarenite and shelly calcarenite..(see p79 Tb. 5 and p87 for more info).||||||07-FEB-11
77197|Cape Burney Sandstone Member|61811|5|Briefly described|p32.|Pleistocene|Pleistocene|||Unit in Tamala Limestone.||Is overlain disconformably by Bootenall Limestone Member.||
74624|Cape Gourdon Formation|64449|2|Defined|p75, p79 Tb. 5, p97-101|Holocene|Holocene|Overlies; Cable Beach Sand, Barn Hill Formation, Shoonta Hill Sand, Mowanjum Sand. Thick: 1.5m. Red, orange and white quartz and quartz-and-carbonate sand, and locally gravelly sand, with small limestone lenses. See p97-101.||||||07-FEB-11
74624|Cape Gourdon Formation|73213|5|Briefly described|958 Fig.3(a), 959, 963, 968|||Alluvial fan deposits at the foot of sea cliffs cut into Mowanjum Sand, from which this unit is derived.||||Overlies Mowanjum Sand. Interfingers with Cable Beach Sand.|Aprons and ribbons of alluvial interlayered sand and muddy sand, or laminated sand. Contains plumes or sheets of shell midden and stone artefact scatters washed from upslope deposits.|19-JAN-23
74050|Cape Hay Formation|13222|6|Mentioned|p229 Fig.2, p234.|||||Unit in Kinmore Group.|||Deltaic sandstones.|
74050|Cape Hay Formation|13242|2|Defined|p214 Fig. 2, p219|Late Permian|Late Permian|Of Mory (1988) - replaced Cape Hay Member (Hyland Bay Fm). Unconf. over Pearce Fm. Now of the Hyland Bay Sub-group (Kinmore Group). Geol. Prov: Bonaparte Basin. Forms the prime upper Palaeozoic sandstone reservoir in this basin. See also p226 Fig. 8. Type section in Petrel 1, 3549-3918 m.||||||21-DEC-12
74050|Cape Hay Formation|64630|5|Briefly described|p31 Fig.2|Capitanian|Wordian|Province: Bonaparte Basin. Unconformably overlies the Pearce Formation. Palynology age: D. parvithola.||||||24-NOV-09
74050|Cape Hay Formation|64690|5|Briefly described|p503-518  |Late Permian|Late Permian|Petrel Field, Bonaparte Basin. This unit is interpreted as a transgressive, sandy tide-dominated, restricted embayment (estuarine) fill succession. The principal gas reservoir unit.||Unit in Hyland Bay Sub-group.||Overlies Pearce Formation. Is overlain by Dombey Formation.|Conglomeratic sandstones with mudstone rip-up clasts; cross-bedded coarse-grained sandstones; fine- to medium-grained sandstones with ripples and cross-bedding; mudstones.|
74050|Cape Hay Formation|64692|6|Mentioned|p522 Fig.2 |Late Permian|Late Permian|Bonaparte Basin.||Unit in Hyland Bay Sub-group.||Overlies Pearce Formation. Is overlain by Dombey Formation.||
74050|Cape Hay Formation|67354|5|Briefly described|p72, p102 Fig.33.|Capitanian|Wordian|||||Overlies Pearce Formation.||
74050|Cape Hay Formation|67370|5|Briefly described|p313, pp315-318. |Permian|Permian|In Fishburn-1 well, there is a shaly interval, assigned to the Penguin Formation, above the eroded top of this unit.||Unit in Hyland Bay Subgroup.||Overlies Pearce Formation. Is overlain by Dombey and Penguin Formations.||
74050|Cape Hay Formation|69452|4|Described|p36:8, 15, 20|Capitanian|Wordian|Bhatia et al. (1984); redefined in Mory (1988) and Gorter (1998). Petrel Sub-basin, Bonaparte Basin. River-dominated delta system with restricted shoreface. Up to 450m thick. Offshore and onshore.||Hyland Bay Subgroup.||Unconformably overlies Pearce Formation. Is overlain unconformably by Dombey Formation.|Thick basal shale overlain by thinly bedded sandstone, siltstone and shale, locally grading into more massive sandstone; unconformably overlain by a thin interval of marine shale, then at least two regressive sandstone-dominated cycles.|12-JUL-16
74050|Cape Hay Formation|69454|5|Briefly described|p38:4|Capitanian|Capitanian|Petrel Sub-basin, Bonaparte Basin.||Hyland Bay Subgroup.||||12-JUL-16
74050|Cape Hay Formation|69653|6|Mentioned|p10|Guadalupian|Guadalupian|Petrel Sub-basin.||Hyland Bay Sub-group.||Overlies Pearce Formation. Is overlain by Dombey Formation.||
74050|Cape Hay Formation|69673|6|Mentioned|p153 fig 125, p173|||||Hyland Bay Subgroup||Overlain by Dombey Formation, overlies Pearce Formation||
74050|Cape Hay Formation|70061|5|Briefly described|Petrel Sub-basin Figs.2 & 3, p2|Capitanian|Capitanian|See also Regional geology: Figs.6-8, p10-11, p16, p19. Vulcan: Fig.2. One of the most prospective hydrocarbon reservoirs within the central Petrel Sub-basin. Marine shales provide an intraformational seal. Hosts gas in anticlinal, fault block and stratigraphic traps (Saratoga 1).||Hyland Bay Subgroup.||Overlies Pearce Formation. Is overlain by Dombey Formation.||12-JUL-16
74050|Cape Hay Formation|70774|5|Briefly described|p5 fig 3|Midian|Kazanian|Bonaparte Basin. [uses superseded age terms]||||||04-JAN-18
74050|Cape Hay Formation|71623|5|Briefly described|p348, 349, 350, p345 fig 2, p346,347,352|Capitanian|Wordian|Bonaparte Basin. Part of Cape Hay Clastic Cycle. Mostly non-marine to deltaic and shallow marine. See also p343.||||Overlies Pearce Formation. Unconformably underlies Dombey Formation.|Sandstone.|08-MAY-19
74050|Cape Hay Formation|72505|5|Briefly described|p890|Wuchiapingian|Wordian|Southern Bonaparte Basin. Correlated to the Didecitriletes ericanus zone to the Dulhuntyispora parvithola zone.||||Overlies the Pearce Limestone. Overlain by the Dombey Formation.||
38678|Cape Leeuwin anorthosite|23788|6|Mentioned|p20|||Geological Province: Yilgarn Craton.||||||
29281|Carawine Dolomite|23354|5|Briefly described|315|||||||||
29281|Carawine Dolomite|23570|5|Briefly described|p143|||Geological Province: Pilbara Craton||||||
29281|Carawine Dolomite|23575|5|Briefly described|Map Legend|Archean|Archean|Of Hamersley Group. Overlain by Pinjian Chert Breccia.||||||07-NOV-08
29281|Carawine Dolomite|23583|5|Briefly described|Map Legend|Archean|Archean|Of Hamersley Group. Geological Province Hamersley Basin.||||||07-NOV-08
29281|Carawine Dolomite|23585|4|Described|p19|Archean|Archean|Age: c.2541+/- 32 Ma (Pb-Pb isochron).  Of Hamersley Group. Overlain by Pinjian Chert Breccia. Underlain by Jeerinah Formation. Geological Province: Hamersley Basin. Max. thickness: >500 m.||||||07-NOV-08
29281|Carawine Dolomite|23594|4|Described|p17|Archean|Archean|Age: >2500 Ma (Jahn and Simonson 1995). Of Hamersley Group. Overlain by Pinjian Chert Breccia. Underlain by Jeerinah Formation. Hamersley Basin. Max. thickness: >500 m.||||||07-NOV-08
29281|Carawine Dolomite|23745|4|Described|p14|Archean|Archean|Of Hamersley Group. Geological Province: Hamersley Basin.||||||07-NOV-08
29281|Carawine Dolomite|23746|4|Described|p20|Archean|Archean|Age: c.2541 Ma. Of Hamersley Group. Geological Province: Hamersley Basin.||||||07-NOV-08
29281|Carawine Dolomite|23813|5|Briefly described|p90 Tb. 1|Archean|Archean|Sedimentary carbonates and clastics.  Age: c.2.603Ga; c.2.56Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.||||||07-NOV-08
29281|Carawine Dolomite|23890|5|Briefly described|p9|Paleoproterozoic|Archean|Of Hamersley Group. Geological Province: Hamersley Basin.||||||07-NOV-08
29281|Carawine Dolomite|23936|5|Briefly described|Tb.1|Archean|Archean|Age: c.2.56 Ga. Geological Province: Pilbara Craton. Of the Hamersley Group.||||||07-NOV-08
29281|Carawine Dolomite|24025|4|Described|p14|Archean|Archean|Of Hamersley Group.  Age: 2541+/-32Ma (Pb-Pb).  Geological Province: Hamersley Basin.||||||07-NOV-08
29281|Carawine Dolomite|24110|5|Briefly described|Plate 1|Archean|Archean|Of the Hamersley Group.   Geological Province: Hamersley Basin||||||07-NOV-08
29281|Carawine Dolomite|29845|6|Mentioned|p125|||||||||
29281|Carawine Dolomite|29850|6|Mentioned|p1020|||||||||
29281|Carawine Dolomite|30437|6|Mentioned|p99|||Refers manganese||||||
29281|Carawine Dolomite|30503|6|Mentioned|p10|||Also mention Table 1||||||
29281|Carawine Dolomite|33544|6|Mentioned|p31|||See also PP280 - 281. Correlates Wittenoom Dol.||||||
29281|Carawine Dolomite|34135|4|Described|Table 2|||Lower Proterozoic. See also pp6,7,12-14.||||||24-JUL-07
29281|Carawine Dolomite|36551|6|Mentioned|p24|||See also Table 23.||||||
29281|Carawine Dolomite|36882|6|Mentioned|p129|||||||||
29281|Carawine Dolomite|37460|6|Mentioned|Fig.3.4|||See also P123||||||
29281|Carawine Dolomite|37707|6|Mentioned|p23|||||||||
29281|Carawine Dolomite|39210|5|Briefly described|p43|||||||||
29281|Carawine Dolomite|39424|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
29281|Carawine Dolomite|39426|4|Described|p12|||||||||
29281|Carawine Dolomite|39444|6|Mentioned|Table 4|||||||||
29281|Carawine Dolomite|39697|4|Described|p125|||||||||
29281|Carawine Dolomite|41622|6|Mentioned|p269|||||||||
29281|Carawine Dolomite|41669|3|Fully described|p28|||||||||
29281|Carawine Dolomite|41768|5|Briefly described|Table 1|||See also p22 and p27.||||||24-JUL-07
29281|Carawine Dolomite|42020|5|Briefly described|p316|||||||||
29281|Carawine Dolomite|42260|6|Mentioned|p127|||||||||
29281|Carawine Dolomite|42352|5|Briefly described|Fig.3 P6|||||||||
29281|Carawine Dolomite|42730|6|Mentioned|p13|||||||||
29281|Carawine Dolomite|43055|4|Described|p17, Table 4|||Of Hamersley Group.||||||24-JUL-07
29281|Carawine Dolomite|43056|5|Briefly described|Map Legend|||of Hamersley Group||||||
29281|Carawine Dolomite|43064|6|Mentioned|p69|||of Hamersley Group||||||
29281|Carawine Dolomite|43595|6|Mentioned|Fig.2-49,p220|||||||||
29281|Carawine Dolomite|43644|6|Mentioned|Table 2,p603|||||||||
29281|Carawine Dolomite|43673|6|Mentioned|p374|||Ejecta age: approx. 2.6 Ga||||||
29281|Carawine Dolomite|44142|6|Mentioned|p316 Tb.4-4, p323|||Hamersley Basin. A paleokarst topography developed on this unit before being covered by Coondoon Formation (Bangemall Group).||||||
29281|Carawine Dolomite|44152|6|Mentioned|p173, p175, p176 Fig.2-154, p178|||||Hamersley Group.||Overlies Lewin Shale. Equivalent to Wittenoom Dolomite.||
29281|Carawine Dolomite|44190|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
29281|Carawine Dolomite|44297|14|Not recorded|p.5,7-10,14,18|||(F51-9).||||||
29281|Carawine Dolomite|44298|14|Not recorded|map legend||Proterozoic|||||||
29281|Carawine Dolomite|44443|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Of Hamersley Group.||||||07-NOV-08
29281|Carawine Dolomite|44503|14|Not recorded|p.7,8,17|||Correlated with Wittenoom Dolomite. (F50-12).||||||
29281|Carawine Dolomite|45923|4|Described|p.67,70,78,79,80-91||Neoproterozoic|Of many pages. Map (F51-5).||||||
29281|Carawine Dolomite|46319|4|Described|p14|Proterozoic|Paleoproterozoic|Of Hamersley Group.  Overlain by Lewin Shale: underlain by Pinjian Breccia.  Maximum thickness: 100m.||||||07-NOV-08
29281|Carawine Dolomite|50287|5|Briefly described|Map Legend|Archean|Archean|Of Hamersley Group (Mount Bruce Supergroup). Age: c. 2541 Ma. Geological Province: Hamersley Basin. Grey-brown recrystallized dolomite with minor shale and chert.||||||07-NOV-08
29281|Carawine Dolomite|50544|4|Described|p52, p15 Tb. 1|Neoarchean|Neoarchean|Of the Hamersley Group. Disconformably overlies the Fortescue Group; unconformably overlain by Pinjian Chert Breccia.  Age: 2541Ma (Pb-Pb, Jahn and Simonson, 1995).  Geological Province: Hamersley Basin.  See also p67.||||||13-OCT-10
29281|Carawine Dolomite|50555|5|Briefly described|Map legend|Archean|Archean|Of the Hamersley Group (Mount Bruce Supergroup).  Massive to well-bedded, recrystallised dolomite and stromatolitic dolomite, minor chert. Overlies Jeerinah Formation; partly underlies Paterson Formation.  Age: c.2541Ma.  Geol.Prov: Hamersley Basin.||||||07-NOV-08
29281|Carawine Dolomite|60635|6|Mentioned|p51 Fig. 2.2A|||||||||
29281|Carawine Dolomite|61560|5|Briefly described|p498 Tb. 4|||Displays impact spherules caused by impact ejecta. Geological Province: Hamersley Basin. See also p500. ||||||
29281|Carawine Dolomite|61575|5|Briefly described|p759|||Of the Hamersley Group. Overlain by Pinjian Chert Breccia; overlies the Jeerinah Formation. Geological Province: Hamersley Basin.||||||
29281|Carawine Dolomite|61576|5|Briefly described|p774 Fig. 1|||Of the Hamersley Group. Contains the Carawine spherule layer. Geological Province: Hamersley Basin.||||||
29281|Carawine Dolomite|61577|5|Briefly described|p787 Tb. 1|Archean|Archean|Age: ca2.56-2.54GA.  Geological Province: east Hamersley Basin||||||07-NOV-08
29281|Carawine Dolomite|62021|5|Briefly described|p169|Proterozoic|Proterozoic|Karstified and contains cavernous zones.||||||
29281|Carawine Dolomite|63139|5|Briefly described|p50|Neoarchean|Neoarchean|Of the Hamersley Group. Overlain by Pinjian Chert Breccia. In the Woodie Woodie area the Hamersley Group is almost entirely Carawine Dolomite.||||||13-OCT-10
29281|Carawine Dolomite|63367|5|Briefly described|p231 Fig.1.|||||Of the Hamersley Group.||||
29281|Carawine Dolomite|63417|5|Briefly described|Map legend|Archean|Archean|Of Hamersley Group (Mount Bruce Supergroup). Overlain by Pinjian Chert Breccia. Age: 2548-2541Ma. Geological Province: Hamersley Basin. Massive to well-bedded, recrystallised dolostone, and stromatolitic dolostone; minor chert.||||||07-NOV-08
29281|Carawine Dolomite|64384|5|Briefly described|p40|||Overlies cherty iron formation (Marra Mamba Fm equiv.) over Jeerinah Fm in eastern part of Hamersley Basin where normal stratigraphic sequence of Hamersley Group has not developed. Stromatolitic carbonate assumed to be equivalent to Wittenoom Dolomite.||||||07-FEB-11
29281|Carawine Dolomite|64580|4|Described|map legend||Neoarchean|Of Lower Hamersley Group. Massive- to well-bedded, recrystallized dolomite, and stromatolitic dolomite; minor chert.||||||15-DEC-08
29281|Carawine Dolomite|64724|5|Briefly described|p42 Fig. 3|Neoarchean|Neoarchean|Sediments of the Hamersley Basin deposited in a continental passive margin setting.||Of Hamersley Group.||||02-APR-12
29281|Carawine Dolomite|65683|5|Briefly described|p799|||Correlated with Wittenoom Dolomite. Shallow water sediments.||||||
29281|Carawine Dolomite|65724|5|Briefly described|map legend|Neoarchaean|Neoarchaean|Of Hamersley Group. Underlies Pinjian Chert Breccia; unconformable under Paterson Formation; over Jeerinah Formation. Dolomite, stromatolitic dolomite; chert. Age: c. 2548 Ma (geochron. JD Woodhead et al, 1988). Geol. Prov: Hamersley Basin, Pilbara Craton||||||
29281|Carawine Dolomite|65757|5|Briefly described|p81 Tb.2, p83|Neoarchean|Neoarchean|in the Hamersley Group, spherule bearing carbonate-chert mega-breccia, 20-30m thick over 100km. Age: 2630+/-6 Ma.||||||
29281|Carawine Dolomite|65825|4|Described|p1, p6, p23, p26.|Archean|Archean|Hamersley Basin. An easterly correlative of the Wittenoom Formation. Deep weathering in the Paleoproterozoic is thought to have led to remobilization and precipitation of manganese, with further supergene enrichment in the Cenozoic.|c.2541 Ma.|Unit in Hamersley Group.||Conformably overlies Fortescue Group.|Grey, recrystallised rock, locally variegated due to iron and manganese impurities, with a variety of shallow-water sedimentary structures; minor shale and nodular chert;|
29281|Carawine Dolomite|65828|5|Briefly described|Map legend|Archean|Archean||c.2541 Ma (Jahn & Simonson).|Unit in Hamersley Group.||Is overlain by Pinjian Chert Breccia.|Grey-brown recrystallised dolomite with minor shale and chert.|04-APR-13
29281|Carawine Dolomite|65829|3|Fully described|p1, p7 Fig.3, p10, pp23-26, p32.|Neoarchean|Neoarchean|Exposed along the southern and western margins of the Ripon Hills. Lower part contains evidence for distal, oceanic impact of an asteroid: chaotic spherule-bearing megabreccia; it contains angular, coarse- to fine-grained dolomite and chert clasts with a microkrystite- and microtectite-rich matrix. Can be correlated with a similar horizon in the Wittenoom Dolomite. Karst weathered. Local occurrences of partly silicified sheets of dissected, secondary carbonate or residual calcrete.|2548 +26/-29 Ma to 2541 +/- 32 Ma.|Unit in Hamersley Group.||Disconformably overlies, or is faulted against, the Jeerinah Formation. Is overlain unconformably by Pinjian Chert Breccia.|Brown-weathering, grey to blue, recrystallised massive and laminated dolomite, intercalated with thin-bedded blue chert and minor shale and siltstone; and an upper evaporite- and stromatolite-bearing shallow-water platform deposit.|
29281|Carawine Dolomite|66887|5|Briefly described|p21 Fig.11|||Pilbara Craton.|~2630-~2625 Ma estimated from Fig.11.|||||
29281|Carawine Dolomite|67130|6|Mentioned|p51, p52 fig 50|Neoarchean|Neoarchean|Contains evidence of an impact event (glass spherules and subsequent tsunami). An identical bed of rocks of identical age in South Africa suggests that this event had a global impact. The Pb-Pb carbonate dates have been regarded as potentially due to a younger recrystallisation event.|2541 +/- 32 Ma - 2541 +/- 18 Ma (Pb/Pb)|||Is equivalent to Wittenoom Dolomite||
29281|Carawine Dolomite|67183|4|Described|p639-46, 649-50,652,655-65,667-8,670-1.|Neoarchean|Neoarchean|Oakover Basin, eastern Pilbara Craton. Flat lying to gently dipping. The Woodie Woodie Mn ore bodies are typically located on or near the unconformity between this unit, the overlying Pinjian Chert Breccia and the Manganese Subgroup. U-Pb date from Rasmussen et al 2005. Pb-Pb isochron ages of 2574-2509 Ma from dolomite thought to represent diagenetic age (Woodhead et al. 1998).|ca2630 Ma SHRIMP U-Pb pyroclastic unit near base|Hamersley Group, Mount Bruce Supergroup||Unconformably underlies Pinjian Chert Breccia, Manganese Subgroup and Stag Arrow Formation; apparent lateral equiv. to Brockman Iron Fm. and Wittenoom Dolomite; conformably overlies Jeerinah Fm.|Mn mineralisation. At Woodie Woodie the dolomite is brown-grey weathered, well-bedded, stromatolitic to massive with interbedded chert (particularly near base). Presence of oncolites, wave ripples and local evaporites.|
29281|Carawine Dolomite|67201|4|Described|p34|||In northeast Hamersley Basin. Shallow-water sedimentary deposit.||Hamersley Group||Stratigraphic equivalent of Wittenoom Formation.|Stromatolitic shallow water carbonate unit.|22-NOV-16
29281|Carawine Dolomite|67202|3|Fully described|p7, p41, p43, p52, p54, p66, p73-74,p119|Archean|Archean|See also p125, p150, p258, p281. Over 500m thick. Deposited in a shallow water platform environment - this is inferred from the presence of sedimentary features. Ore host. Bores intersecting this aquifer supply water for the Woodie Woodie mining community. The irregular upper surface may represent a palaeokarst. Hosts Mn deposits in karstic depressions. Poorly magnetised: not discriminated in aeromagnetic data. Age is a Pb-Pb isochron date regional metamorphism or early diagenesis. May have massive, nodular and cavernous calcrete formed in situ, or a silcrete duricrust locally. Shown on p258 as unit in Fortescue Group.|c.2540 Ma (Jahn and Simonson, 1995).|Hamersley Group.||Disconformably overlies Jeerinah Formation (Fortescue Group). Is overlain unconformably by Pinjian Chert Breccia and Waltha Woora Formation.|Grey dolomite with minor shale and chert interbeds.|15-FEB-18
29281|Carawine Dolomite|67229|6|Mentioned|p3 Fig.2|||Noldart and Wyatt (1962), in mapping this unit, included rocks later named (de la Hunty, 1964) the Lewin Shale (lower part), and subsequently the Jeerinah Formation (MacLeod and de la Hunty, 1965).||||||
29281|Carawine Dolomite|67829|5|Briefly described|pp447-449, p453.|||East Pilbara. Equivalent of Wittenoom Formation in the Hamersley Basin. Shallow-water deposits. Underwent deep and extreme Precambrian karsting which continued after deposition of Manganese Group, which locally infills "box" synclines in this unit.||||Is overlain by Manganese Group.||
29281|Carawine Dolomite|68035|6|Mentioned|p293|||Hamersley Basin, east Pilbara. Abundantly stromatolitic.||||||
29281|Carawine Dolomite|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Hamersley Group||Overlain by Pinjian Chert Breccia|Massive- to well-bedded, recrystallized dolomite, and stromatolitic dolomite; minor chert. Spherule bearing megabreccia; angular, coarse to fine grained dolomite and chert clasts with a microkrystite and microtectite rich matrix.|
29281|Carawine Dolomite|69185|4|Described|GEOL_LUT_CSV files||Neoarchean|Geological Province: Pilbara Craton. Of Northeast Pilbara Sub-basin, Hamersley Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.||Unit of Hamersley Group.||Overlain by Pinjian Chert Breccia.|Massive- to well-bedded, recrystallized dolomite, and stromatolitic dolomite; minor chert|
29281|Carawine Dolomite|69563|5|Briefly described|p689-691, p695-698|||Contains a 20-30m thick spherule-bearing megabreccia: asteroid impact ejecta.|2630 +/- 6 Ma.|||||
29281|Carawine Dolomite|69590|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Of Hamersley Basin. Events: Paterson Orogeny; Miles Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_geologyp08_lut.csv, 250k_interpgeol_lut.csv.|2630-2504 Ma (isotopic; inferred)|Unit of Hamersley Group.|||Massive- to well-bedded, recrystallized dolomite, and stromatolitic dolomite; chaotic spherule-bearing megabreccia; angular, coarse- to fine-grained dolomite and chert clasts with a microkrystite- and microtectite-rich matrix.|
29281|Carawine Dolomite|70733|6|Mentioned|p108, 112, 116, 120|||Also appears as Carawine breccia or Carawine Dolomite megabreccia. Comparison of tektite fragments, PGE values, with those in Marble Bar Chert Member.|||||Megabreccia, with blocks of carbonate and chert.|
29281|Carawine Dolomite|70826|6|Mentioned|p8|Neoarchean||||||Overlain by the Pinjian Chert Breccia.||
29281|Carawine Dolomite|71042|4|Described|p63, p64 fig 1, p65-p69|Neoarchean|Neoarchean|Southern Pilbara. Interpreted as a carbonate platform deposited in shallow water on the basis of abundant stromatolites, oncolites, wave ripples and local evaporates (there are however deeper facies present in some places). Equivalent to the Brockman Iron Formation and the Wittenoom Formation. A SHRIMP U-Pb date of ca 2630 (Rassmussen et al., 2005) has been derived from a pyroclastic unit near the base of this formation and Pb-Pb isochron ages from the dolomite ranging from 2574 to 2509 are thought to be diagenetic ages for the same unit (Wood et al., 1998). See also p71-p83, p85-p86, p88-p91, p94-p95, p97-p98, p100.|ca 2630 Ma|Hamersley Group||Conformably overlies the Jeerinah Formation (Fortescue Group). Overlain by the Pinjian Chert Breccia. Unconformably overlain by the Manganese Group, Coondoon Formation and the Googenhama Formation.|Brown-grey, weathered, well-bedded, stromatolitic to massive dolomite.|
29281|Carawine Dolomite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||crystalline dolostone/dolomite|
29281|Carawine Dolomite|71513|6|Mentioned|p73, p89|||Cross-cut in part by hydrothermal veins of calcite, chlorite, hematite and magnetite in the east Hamersley Province.||||||
29281|Carawine Dolomite|71808|5|Briefly described|p6, p10, p37-p39, p44, p98, p101-p102|||Oakover Sub-basin. Peritidal to deep marine depositional environments.|||||Stromatolitic to moderately deep water carbonates.|
29281|Carawine Dolomite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Carawine Sub-basin, Hamersley Basin.||Hamersley Group, lower||Overlain by Pinjian Chert Breccia.|Massive- to well-bedded, recrystallized dolomite, and stromatolitic dolomite; minor chert.|
41170|Carbana Monzogranite|50381|5|Briefly described|Map Legend|Archean|Archean|Of Corunna Downs Granitoid Complex.  Geological Province: Pilbara Craton.  Age: 3317-3313 Ma||||||07-NOV-08
41170|Carbana Monzogranite|63417|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite.  Age: 3311 Ma. Geological Province: Pilbara Craton. Biotite monzogranite; porphyritic, local mafic xenoliths; metamorphosed.||||||15-APR-13
41170|Carbana Monzogranite|63441|5|Briefly described|p8 Tb. 2|Archean|Archean|Of Emu Pool Supersuite. Supersedes Carbana Pool Adamellite. Age range: 3317 +/- 2 Ma to 3313 +/- 9 Ma. Geological Province: Pilbara Craton.||||||15-APR-13
41170|Carbana Monzogranite|64327|5|Briefly described|p61|Archean|Archean|Previously called "Carbana Pool Adamellite". Redefined unit now includes granitic rocks forming most of northern 2/3 of Corunna Downs Granitoid Complex. Ages range: 3317 +/- 2 Ma to 3313 +/- 9 Ma (SHRIMP U-Pb). Detailed lith. given, including its syentite centre.||||||15-APR-13
41170|Carbana Monzogranite|64621|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite. Age: 3317-3313 Ma. Biotite monzogranite; feldspar porphyritic, common mafic xenoliths; weakly metamorphosed.||||||15-APR-13
41170|Carbana Monzogranite|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Corunna Downs Granitoid Complex. Geological Province: Pilbara Craton. Hornblende monzogranite; fine to medium grained, even grained to slightly porphyritic; metamorphosed.||||||07-FEB-11
41170|Carbana Monzogranite|65008|5|Briefly described|p7, p12, p41|Paleoarchean|Paleoarchean|East Pilbara Granite-Greenstone Terrane. Geochronology by Barley and McNaughton (1998).|3317-3313 Ma|Of the Corunna Downs Granitoid Complex.|||Fine- to medium-grained, equigranular to slightly porphyritic hornblende monzogranite. Consists of quartz, altered plagioclase and biotite, disseminated hornblende, and accessory epidote, titanite, and apatite.|14-MAY-14
41170|Carbana Monzogranite|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton. Mapped as three sub-units.|c.3317 - 3313 Ma (Barley and Pickard 1999).|Of Corunna Downs Granitoid Complex.|||Biotite monzogranite, fine- to coarse-grained, sparsely feldspar porphyritic; hornblende monzogranite, equigranular to slightly porphyritic; biotite monzogranite to granodiorite, weakly foliated, minor pegmatite.|
41170|Carbana Monzogranite|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. |c.3311 Ma.|Of Emu Pool Supersuite.|||Biotite monzogranite, feldspar porphyritic, common mafic xenoliths; hornblende monzogranite, fine- to medium-grained, equigranular to slightly porphyritic. Metamorphosed.|
41170|Carbana Monzogranite|65827|3|Fully described|p6 Tb.2, p9 Fig 3, p13 Tb.4, p24-25|Paleoarchean|Paleoarchean|Of Emu Pool Supersuite. 3311+/-3 Ma (SHRIMP U-Pb zircon; Nelson et al. 2006). Adjacent to/intrudes Panorama Formation; faulted against by Euro Basalt; intruded by Mondana Monzogranite. Of Corunna Downs Granitic Complex. Biotite monzogranite to granodiorite, hornblende monzogranite.||||||
41170|Carbana Monzogranite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Emu Pool Supersuite. 3317-3307 Ma. Biotite monzogranite; feldspar porphyritic; common mafic xenoliths; weakly metamorphosed.||||||
41170|Carbana Monzogranite|69012|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane.|c. 3313 Ma|Of the Emu Pool Supersuite.|||Comprises biotite monzogranite; feldspar porphyritic; common mafic xenoliths; weakly metamorphosed.|
41170|Carbana Monzogranite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Alternatively called Carbana Adamellite. Age derived from samples of monzogranites (142978.1.pdf, 169027.1.pdf)|3307 +/- 4 Ma -  3315 +/- 6 Ma (SHRIMP)|Emu Pool Supersuite|||Granodiorite to biotite monzogranite; feldspar porphyritic; common mafic xenoliths; weakly metamorphosed. Strongly foliated metagranite and granitic schist. Hornblende monzogranite, leucogranite and syenogranite.|
41170|Carbana Monzogranite|69566|6|Mentioned|p236|||Corunna Downs Granitoid Complex, East Pilbara Granite-Greenstone Terrane.||||||
41170|Carbana Monzogranite|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Also referred to as Carbana Adamellite (Hickman 1983). Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA 142978 (monzogranite) yielded an interpreted igneous crystallisation age of 3307+\-4 Ma for the monzogranite (weighted mean 207Pb/206Pb). Sample GSWA 169027 (biotite monzogranite) yielded an interpreted igneous crystallisation age of 3315+\-6 Ma for the monzogranite (weighted mean 207Pb/206Pb). Sample GSWA 169028 (porphyritic bt-hbl monzogranite) yielded an interpreted igneous crystallisation age of 3314+\-4 Ma for the monzogranite (weighted mean 207Pb/206Pb). Sample GSWA 178084 bt-hbl monzogranite) yielded an interpreted igneous crystallisation age of 3311+\-3 Ma for the monzogranite (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.|3317-3311 Ma (inferred; isotopic)|Unit of Emu Pool Supersuite.|||Biotite monzogranite to granodiorite to syenogranite, hornblende monzogranite, leucogranite, metagranite, granitic schist.|
41170|Carbana Monzogranite|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||monzogranite, granite, syenogranite, granodiorite|
41170|Carbana Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||Max age 3317+/-2 Ma, min 3310+/-4 Ma.|Emu Pool Supersuite|||Biotite monzogranite; feldspar porphyritic; common mafic xenoliths; weakly metamorphosed.|
41170|Carbana Monzogranite|73598|6|Mentioned|p1208 Fig.1, 1209, 1213|Paleoarchean|Paleoarchean|East Pilbara Terrane. Near the Kelly Dyke swarm.|3313 +/- 9 Ma.|||||
70159|Cardinal Formation|63441|2|Defined|p4 Tb. 1, p21|Archean|Archean|Base of Soanesville Gp (Pilbara Supergp) - newly ascribed (Van Kranendonk 2006) to upper, red-weathering grey shale component of former Pincunah Hill Fm.Thickness: ~700m. Conformable/disconform. over Kangaroo Caves Fm; conform/disconform.below Corboy Fm.||||||07-FEB-11
70159|Cardinal Formation|64405|5|Briefly described|p4 Fig. 3|Archean|Archean|Name inferred from Cardinal only in Figure 3. Of the Soanesville Group (De Grey Supergroup). Sedimentary.||||||07-FEB-11
70159|Cardinal Formation|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Unit in Soanesville Group. Red-weathered, ferruginized black shale, with minor siltstone; local banded iron-formation, chert, sandstone and conglomerate; metamorphosed.||||||
70159|Cardinal Formation|66745|5|Briefly described|p53 Fig.3.|Mesoarchean|Mesoarchean|||Unit in Soanesville Group.||Shown as overlying Budjan Creek Formation. Is overlain by Corboy Formation.|Shale.|12-OCT-15
70159|Cardinal Formation|67130|5|Briefly described|p16|||||Soanesville Group||Overlain by Corboy Sandstone|Shale.|
70159|Cardinal Formation|67197|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Soanesville Group.||||
70159|Cardinal Formation|67201|5|Briefly described|p12 Tb.1|||In northern Pilbara Craton, East Pilbara Terrane, Soanesville Basin, rift-related successions.||Soanesville Group||||
70159|Cardinal Formation|67668|6|Mentioned|Fig. 2; p. 154||Mesoarchean|East Pilbara Terrane, Pilbara Craton.||Soanesville Group||Underlies the Corboy Formation, overlies the Sulphur Springs Group (Kangaroo Caves Formation).|Clastic sediments.|
70159|Cardinal Formation|68282|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.||Of the Soanesville Group|||Red-weathered, ferruginised black shale, with minor siltstone, local banded iron formation, chert, sandstone, and conglomerate, metamorphosed; secondary chert; schistose metafelsic volcanic rocks, quartz-sericite schist; silicified shale.|
70159|Cardinal Formation|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|Pilbara Craton. Also includes 2 unnamed sub-units mapped separately: silicified shale with variegated, layered secondary chert, metamorphosed; and secondary chert from silicification of fine-grained felsic volcaniclastic rocks, with layered white, grey and cream chert.||Of the Soanesville Group.|||Red-weathered, ferruginised black shale with minor siltstone; local banded iron-formation, chert, sandstone and conglomerate; all metamorphosed.|02-MAY-14
70159|Cardinal Formation|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Soanesville Group|||Ferruginized shale, banded iron-formation, chert, sandstone, and conglomerate; metamorphosed. Schistose metafelsic volcanics; quartz sericite schist includes local psammite and metachert. Silicified shale, variegated, layered secondary chert.|
70159|Cardinal Formation|69301|5|Briefly described|p9 Tb.1|||Pilbara Craton. East Pilbara Terrane. Budjan Creek Basin. Rift-related successions.||Soanesville Group||||
70159|Cardinal Formation|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Paleoarchean|Geological province: Pilbara Craton. Of Soanesville Basin. Events: Mosquito Creek Orogeny; North Pilbara Orogeny; Prinsep Orogeny; East Pilbara Terrane Rifting Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.|3228-3176 Ma (inferred)|Unit of Soanesville Group.|||Red-weathered, ferruginized black shale, minor siltstone; local banded iron-formation, chert, sandstone, and conglomerate; metamorphosed; Schistose metamorphosed felsic volcanic rock; quartz-sericite schist; includes local psammite and metachert.|
70159|Cardinal Formation|69616|6|Mentioned|p161|Archean|Archean|||Unit in Soanesville Group.||Overlies Sulphur Springs Group. Is overlain by Corboy Formation.||
70159|Cardinal Formation|70775|5|Briefly described|p12|||East Pilbara.||Soanesville Group||Overlain by the Corboy Formation.||
70159|Cardinal Formation|71267|6|Mentioned|1m_geologyl12_lithology_lut.csv||||||||banded iron formation|
70159|Cardinal Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Paleoarchean|Soanesville Basin.||Soanesville Group|||Black shale with minor siltstone; local banded iron-formation, chert, sandstone, and conglomerate; metamorphosed.|
70159|Cardinal Formation|72668|5|Briefly described|p5-6|||East Pilbara Terrane.||Soanesville Group||Overlain by the Corboy Formation.|Shale.|
75852|Cardunia Rocks Monzogranite|64775|5|Briefly described|p6-1|Neoarchean|Neoarchean||2638 +/- 26 Ma SHRIMP.||||Fractionated hornblende bearing, leucocratic body with fluorite and cassiterite.|30-MAR-12
78995|Carlaminda Komatiite Member|70226|5|Briefly described|Map legend.|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Carton.|c. 2793 Ma.|Yalgoo Formation|||Volcaniclastic sandstone to siltstone (rhyolitic to dacitic); peridotite; olivine spinifex-textured komatiite; pyroxene spinifex-textured basalt; tremolite-chlorite-actinolite+/-talc schist; serpentinite (from volcanics); sheared; metamorphosed.|16-DEC-15
78995|Carlaminda Komatiite Member|70796|5|Briefly described|100k_geologyl_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, Yalgoo100_2241_stratig.pdf. Numerous additional lithologies are discussed.|ca 2800 to 2793 Ma (inferred)|Yalgoo Formation|||Platy olivine spinifex textured komatiite, moderately wellbedded volcaniclastic sandstone to siltstone of rhyolitic to dacitic affinity, peridotite. Tremolitechloriteactinolitetalc schist with minor serpentinite.|
78995|Carlaminda Komatiite Member|70830|5|Briefly described|p58|||Youanmi Terrane.||||||
78995|Carlaminda Komatiite Member|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. See 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeol_lut.csv.|2800-2793 Ma|Unit of Yalgoo Formation.|||Tremolite-chlorite-actinolite+\-talc schist, minor serpentinite; locally strongly sheared, platy olivine spinifex-textured komatiite; randomly oriented plates of serpentine after olivine; flows of pyroxene spinifex-textured basalt; metamorphosed.|
40564|Carnac Formation|12758|4|Described|p20, p10 Fig.10|Early Cretaceous|Early Cretaceous|Supersedes the Carnac Member (Parmelia Formation). Now of the Parmelia Group. Includes three members: Stragglers, Mangles and Hawley Members. Also now contains the former informal "X Shale" and "Y Shale" of Devereux (1993). See also p18.||||||27-JUL-09
40564|Carnac Formation|14227|5|Briefly described|Enclos. 2|Berriasian|Berriasian|Of Parmelia Group. Includes Hawley, Mangles and Stragglers Members. Underlies Charlotte Sandstone. Presented as Carnac Fm.||||||07-FEB-11
40564|Carnac Formation|24443|5|Briefly described|Fig.31|Early Cretaceous|Late Jurassic|Of Parmelia Group. Conformably overlies Jervoise Sandstone. Conformably overlain by Charlotte Sandstone. Geological Province: Perth Basin.||||||
40564|Carnac Formation|50108|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Parmelia Group.  Geological Province: Perth Basin.||||||
40564|Carnac Formation|60376|5|Briefly described|p17 Fig. 4.|Late Jurassic|Late Jurassic|Geological Province: Perth Basin. Of the Parmelia Group. Overlain by Charlotte Sandstone. Underlain by Jervoise Sandstone.||||||07-FEB-11
40564|Carnac Formation|69182|6|Mentioned|Ch2 p15|Lower Cretaceous|Lower Cretaceous|Perth Basin. ||Parmelia Group|Includes the Stragglers, Mangles and Hawley Members.|||
40564|Carnac Formation|69297|6|Mentioned|p175, p176, p189|Berriasian|Tithonian|Vlaming Sub-basin, South Perth Basin. ||Parmelia Group||||
40564|Carnac Formation|70097|5|Briefly described|p9, p19 Fig.3|Berriasian|Berriasian|Southern Perth Basin. Vlaming Sub-basin and Bunbury Trough. On p19 Fig.3, misspelt as Cormac Formation.||Parmelia Group|Stragglers Member||Includes sandstone.|
40564|Carnac Formation|70099|5|Briefly described|Fig.4; p5|Berriasian|Berriasian|Vlaming Sub-basin. Correlated to Mentelle 3 syn-rift Supersequence.||Parmelia Group.||||
40564|Carnac Formation|70128|5|Briefly described|p463 Fig.10|Early Cretaceous|Early Cretaceous|Vlaming Sub-basin.||Parmelia Group.|Mangles Member.|Overlies Jervoise Sandstone.||
40564|Carnac Formation|71377|5|Briefly described|p7|Early Cretaceous|Late Jurassic|Bunbury Trough, Perth Basin.||Parmelia Group||||
40564|Carnac Formation|71958|5|Briefly described|p14-p15, p34, p41|Tithonian|Kimmeridgian|Vlaming Sub-basin. See also p45-p46, p51, p80, p98.||Parmelia Group|Includes the Stragglers Member, Hawley Member and Mangles Member.|Unconformably overlain by the Warnbro Group. Overlies the Jervoise Sandstone. Overlain by the Charlotte Sandstone.|Shales, siltstone and thin sandstones.|
24214|Carolyn Formation|7433|5|Briefly described|pp34-35.|Sakmarian|Sakmarian|Fitzroy Sub-basin, Canning Basin. ||Unit in upper Grant Group.||Is overlain by Nura Nura Member and, locally, Tuckfield Member.|Non-marine, deltaic and minor shallow marine clastics.|
24214|Carolyn Formation|22718|6|Mentioned|P5|||||||||
24214|Carolyn Formation|22738|5|Briefly described|12|Early Permian|Early Permian|Parent Grant Group. Underlying unit Winifred Formation.||||||10-NOV-08
24214|Carolyn Formation|22741|6|Mentioned|P25|Early Permian|Late Carboniferous|||||||
24214|Carolyn Formation|22753|6|Mentioned|p535|||Obsolete subdivision of Grant Group.||||||10-NOV-08
24214|Carolyn Formation|22765|6|Mentioned|P10||Permian|||||||
24214|Carolyn Formation|22767|5|Briefly described|Table3 P16, P21||Early Permian|||||||
24214|Carolyn Formation|22776|6|Mentioned|Table.3|Early Permian|Early Permian|Grant Group||||||
24214|Carolyn Formation|23212|5|Briefly described|Table.1 p7||Sakmarian|Of Grant Group.||||||10-NOV-08
24214|Carolyn Formation|23765|5|Briefly described|Map Legend|Permian|Carboniferous|||||||23-DEC-09
24214|Carolyn Formation|23766|4|Described|p14 Tb. 2|Early Permian|Early Permian|Consists of sandstone, conglomerate and shale. Parent: Grant Group. Thickness: 250m.  See also p19.||||||10-NOV-08
24214|Carolyn Formation|36224|5|Briefly described|Map legend|Early Permian|Early Permian|Of the Grant Group.  Includes the Wye Worry and Millajiddee Members.  Mainly sandstone; minor conglomerate.||||||01-FEB-05
24214|Carolyn Formation|36225|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
24214|Carolyn Formation|36634|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
24214|Carolyn Formation|37914|4|Described|p449|||||||||08-FEB-10
24214|Carolyn Formation|41158|5|Briefly described|p80|||Mention p207.||||||20-FEB-20
24214|Carolyn Formation|41215|6|Mentioned|p281|||||||||
24214|Carolyn Formation|41315|6|Mentioned|p135|||||||||
24214|Carolyn Formation|41839|4|Described|p26|||||||||
24214|Carolyn Formation|42392|6|Mentioned|p119|||||||||
24214|Carolyn Formation|42547|4|Described|p97|||Part of Grant Group.||||||
24214|Carolyn Formation|42613|2|Defined|p10|Sakmarian|Sakmarian|Of Grant Group.||||||10-NOV-08
24214|Carolyn Formation|42734|5|Briefly described|map legend|Permian||||||||
24214|Carolyn Formation|43015|5|Briefly described|Table 1,p319|||Of Grant Group.||||||10-NOV-08
24214|Carolyn Formation|43563|6|Mentioned|Fig.9,p15||Early Permian|||||||
24214|Carolyn Formation|43816|5|Briefly described|Fig.2,p88|||||||||
24214|Carolyn Formation|43818|6|Mentioned|p38|||||||||
24214|Carolyn Formation|44143|4|Described|p.436 Table 4-19; p.446|Permian|Permian|Unit in Grant Group. Up to 415m thick; sandstone, conglomerate, and mudstone; dropstones and tillites; non-marine and marine glacial. Conformably overlies Winifred Formation. Composite section details given.||||||22-NOV-17
24214|Carolyn Formation|45158|4|Described|p22|||||||||
24214|Carolyn Formation|49644|5|Briefly described|Table|||||||||
24214|Carolyn Formation|64502|5|Briefly described|p766 Fig.3, p768 Fig.5, p 769, Fig.6||Early Permian|Of Grant Group.Includes Ngumban Claystone Member and Deeadeea Sandstone Member in Lennard Shelf region.||||||10-NOV-08
24214|Carolyn Formation|64630|5|Briefly described|p31 Fig.2, p33, 35, 37|Sakmarian|Sakmarian|Province: Northern and Central Canning Basin.  Of Grant Group in Fitzroy Trough area. Underlies the Poole Sandstone, overlies the Winifred Formation, equivalent to Clianthus, Calytrix and Hoya formations. Palynology age: P. confluens.||||||24-NOV-09
24214|Carolyn Formation|64643|5|Briefly described|p8|Sakmarian|Sakmarian|Of Grant Group in Fitzroy Trough. Includes the Wye Worry and Ngumban, Millajiddee and Deeadeea Members.||||||24-NOV-08
24214|Carolyn Formation|64971|5|Briefly described|p685 Fig. 2|Early Permian|Early Permian|||||||09-FEB-10
24214|Carolyn Formation|64974|5|Briefly described|p148 Fig. 6|Sakmarian|Sakmarian|Of Grant Group. Geological Province: Canning Basin.||||||17-JUN-09
24214|Carolyn Formation|64981|5|Briefly described|p669 Fig.3.|Sakmarian|Sakmarian|||Unit in Grant Group.||Overlies Winifred Formation. Is overlain by Poole Sandstone.|Non-marine sandstones and shales.|
24214|Carolyn Formation|64982|5|Briefly described|pp699-700.|||||Unit in Grant Group.|||Sandstone, conglomerate and mudstone.|
24214|Carolyn Formation|65486|5|Briefly described|p4, p18, p55|Early Permian|Early Permian|Basal formation of Grant Group, Canning Basin. Contains Ngumban Claystone, and Deeadeea Sandstone, Members. Unconformably overlies Prices Creek Group, Fairfield Group.||||||
24214|Carolyn Formation|66127|3|Fully described|p8, p61, pp212-213. |Early Permian|Early Permian|Largely removed by Mesozoic and Cenozoic erosion.||Unit in Grant Group.|Includes Ngumban Claystone and Deeadeea Sandstone Members.|Locally overlies Bugle Gap and Pillara Limestones, Prices Creek Group and Fairfield Group with a Permian glacially-planed unconformity.|Glacigene shale, diamictite and sandstone.|
24214|Carolyn Formation|66949|4|Described|p8, p10-11, p13-14, p16-17, p20|Sakmarian|Asselian|See also p52,54 Appx.2, p57 Appx.3, p60-65 Appx.4; p76-78,81,83,85-86,88-90,93 Appx.5; Plates 2-12. Composite section detailed. Up to 415m thick; non-marine and marine glacial deposits. Rare marine macrofossils: Eurydesma and Deltopecten lyonensis. Available core and Formation picks detailed.||Unit in Grant Group.|Includes Millajiddee, Wye Worry, Deeadeea Sandstone, Ngumban Claystone, Members.|Conformably overlies Winifred Formation.|Sandstone, conglomerate and mudstone.|30-OCT-15
24214|Carolyn Formation|68007|4|Described|p2, p9, p12, Plates 1, 2|Permian|Permian|Southern Canning Basin. 190.5m thick in Patience 2 well. Composite well log. Menzel and Lipski (1986) previously assigned the upper part of the presently recognised Carolyn Formation to the lower Poole Sandstone in Patience 1. Palynomorphs recovered from cuttings over 873 to 1323 m in Patience 1 are assigned to the P. confluens Zone, which is characteristic of the Grant Group (Backhouse, 1997).||Grant Group.||Overlies Winifred Formation. Is overlain by Poole Sandstone. Equivalent to Clianthus Formation.|Interbedded sandstone, siltstone and claystone in varying proportions.|20-FEB-20
24214|Carolyn Formation|69693|5|Briefly described|p3-10|Sakmarian|Sakmarian|Lennard Shelf, Canning Basin. Seismic interpretation detailed. See also references to Carolyn formation (p1-2, 4, 6, 8, 10).||||Overlies Winifred Formation. Is overlain unconformably by Poole Sandstone. Equivalent to Clianthus Formation.|Sandstone and mudstone.|
24214|Carolyn Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Grant Group.|||Conglomeratic sandstone, sandstone, siltstone, laminated calcareous siltstone, claystone, mudstone with calcareous concretions and faceted and striated dropstones. Wood fragments, trace fossils and bioturbations, and palynomorphs.|
24214|Carolyn Formation|72496|5|Briefly described|p217-218, p220, p222-223, |Sakmarian|Sakmarian|Canning Basin, Lennard Shelf. Thickness ranges between 63 to 386.4m in wells. Deposited in a glacial marine to shallow water environment. Exhibits variable seismic characteristics. See also p226-228, p230-231.||Grant Group||Equivalent to  the Clianthus Formation. Overlies the Winifred  Formation.|Massive and cross-bedded sandstone with thin mudstone intervals.|19-MAR-20
24214|Carolyn Formation|72497|4|Described|p1, p4-5, p8, p10, 18-19, 24-25, 28.|Sakmarian|Asselian|Outcrops along the St George Ranges Anticline, Mount Anderson and Mount Bannerman areas in the northern Canning Basin. After Crowe and Towner, 1976. Vertical and lateral facies variations and stratigraphic relationships discussed. Outcrops in the George Ranges Anticline, however the stratigraphic relationships are yet to be determined.||Grant Group|Includes Millajiddee Member and Wye Worry Member.|Overlies Grant Group and Millajiddee Member.|Includes siltstone, claystone, horizontally laminated sandstone and massive sandstone with dropstones. Deltaic sediments deposited within a channel environment.|
24214|Carolyn Formation|72499|4|Described|p43, p54 Fig.48, p93.|Cisuralian|Cisuralian|Associated facies recorded on well logs Sundown 1 and Sundown 3/3H (Lennard Shelf), The Sisters 1 and Scarpia 1 (Fitzroy Trough), Frome Rocks 2 (Jurgurra Terrace), Dampier Downs 1 and Roebuck Bay 1 (Broome Platform) and Perindi 1 (Pender Terrace).||Grant Group||Overlies Winifred Formation and underlies Poole Sandstone.|Includes diamictites, turbidites and mudstone, with fluvial-shallow marine sandstone, cross-bedded sandstone.|
24214|Carolyn Formation|73117|4|Described|p22-23, p25, p117, p125, p136|||Of Crowe and Towner (1975, 1976). [Written as Carolyn Formation, 'Carolyn Formation' and 'Carolyn' ... Formations]. Part of the 'three ladies' naming scheme proposed as a subdivision of the Grant Group. Authors consider this an informal unit. This scheme for constituents of the Grant Group has been widely applied but is considered flawed by the authors because of spatially isolated type sections. Known from outcrop; not readily identified in the subsurface. No obvious base has been identified.||Grant Group|Wye Worry Member, Millajiddee Member|||
27365|Carrandibby Formation|23174|5|Briefly described|Fig5p8|Early Permian|Early Permian|||||||
27365|Carrandibby Formation|23311|6|Mentioned|map legend|||||||||
27365|Carrandibby Formation|23312|6|Mentioned|map legend|||Included in Lyons Formation.||||||
27365|Carrandibby Formation|23726|5|Briefly described|p37|Early Permian|Early Permian|Of Lyons Group. Overlying unit Callytharra Formation. Underlying unit Harris Sandstone. Geological Province: Carnarvon Basin.||||||
27365|Carrandibby Formation|23815|4|Described|p280|Sakmarian|Sakmarian|Geological Province: Carnarvon Basin. Underlying unit: Lyons Group (conformable). Overlying unit: Callytharra Formation. Max thickness: 72 m. Contains many marine fossils.||||||
27365|Carrandibby Formation|24044|5|Briefly described|p541 Fig.2|Early Permian|Early Permian|||||||
27365|Carrandibby Formation|30341|6|Mentioned|p145|||||||||
27365|Carrandibby Formation|30545|6|Mentioned|Fig.2|||Sakmarian||||||
27365|Carrandibby Formation|32648|6|Mentioned|p32|||Sakmarian||||||
27365|Carrandibby Formation|32945|6|Mentioned|p73|||See also P87. Permian||||||
27365|Carrandibby Formation|33594|6|Mentioned|p37|||||||||
27365|Carrandibby Formation|33701|6|Mentioned|Fig.1|||Sakmarian||||||
27365|Carrandibby Formation|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
27365|Carrandibby Formation|34999|6|Mentioned|p124|||||||||
27365|Carrandibby Formation|36020|6|Mentioned|p389|||||||||
27365|Carrandibby Formation|36890|3|Fully described|p280|||||||||
27365|Carrandibby Formation|37295|4|Described|p52|||See also Table 2.||||||
27365|Carrandibby Formation|37920|5|Briefly described|p453|||||||||
27365|Carrandibby Formation|38217|5|Briefly described|p269|||||||||
27365|Carrandibby Formation|38493|4|Described|p34|||||||||
27365|Carrandibby Formation|38494|4|Described|p29|||||||||
27365|Carrandibby Formation|40336|5|Briefly described|p18|||||||||
27365|Carrandibby Formation|40339|6|Mentioned|Map legend|Sakmarian|Sakmarian|||||||
27365|Carrandibby Formation|40340|6|Mentioned|Table 2|||||||||
27365|Carrandibby Formation|40343|6|Mentioned|Table 1|||||||||
27365|Carrandibby Formation|40617|6|Mentioned|p13|||Mention Fig.1||||||
27365|Carrandibby Formation|41053|6|Mentioned|Fig.2|||||||||
27365|Carrandibby Formation|41271|3|Fully described|p74|||||||||
27365|Carrandibby Formation|41315|6|Mentioned|p149|||||||||
27365|Carrandibby Formation|41438|6|Mentioned|Fig.11|||||||||
27365|Carrandibby Formation|41839|6|Mentioned|p20|||||||||
27365|Carrandibby Formation|42116|4|Described|p27|||||||||
27365|Carrandibby Formation|42392|5|Briefly described|p115|||||||||
27365|Carrandibby Formation|42547|6|Mentioned|p91|||||||||
27365|Carrandibby Formation|43015|5|Briefly described|Table 1,p319|||||||||
27365|Carrandibby Formation|43018|5|Briefly described|Table 1,p386|||of Lyons Group||||||
27365|Carrandibby Formation|43255|5|Briefly described|map legend||Sakmarian|||||||
27365|Carrandibby Formation|43256|5|Briefly described|18,22||Permian|||||||24-NOV-09
27365|Carrandibby Formation|43474|14|Not recorded|p25||Sakmarian|Upper Sakmarian||||||
27365|Carrandibby Formation|43835|5|Briefly described|Map Legend||Sakmarian|||||||
27365|Carrandibby Formation|44040|14|Not recorded|p44|||||||||
27365|Carrandibby Formation|44217|14|Not recorded|Fig.3|||||||||
27365|Carrandibby Formation|44219|14|Not recorded|p31||Sakmarian|Upper pt. of Lyons Group.||||||
27365|Carrandibby Formation|44344|14|Not recorded|p.9|||Sakmarian fauna. (G50-1).||||||
27365|Carrandibby Formation|44532|4|Described|p.4,6, map|||(G50-5).||||||
27365|Carrandibby Formation|44533|5|Briefly described|map legend|||Artinskian (?)||||||
27365|Carrandibby Formation|44994|6|Mentioned|Fig.7|||Correlation.||||||
27365|Carrandibby Formation|45016|2|Defined|p57-60|Artinskian|Sakmarian|Tb, p.18,25,Fig.56, p.50,53,55,62-64,69,110, Fig.65. Artinskian or Sakmarian (G50-5,6).||||||09-AUG-06
27365|Carrandibby Formation|46849|6|Mentioned|Fig. 6|||||||||
27365|Carrandibby Formation|47041|6|Mentioned|Fig.2|||||||||
27365|Carrandibby Formation|48885|14|Not recorded|p.1,2,7-9,Pl.1||Early Permian|Lower Permian (Sakmarian-Artinskian). (G/50-6).||||||
27365|Carrandibby Formation|49644|5|Briefly described|Table|||||||||
27365|Carrandibby Formation|60296|5|Briefly described|p156 Fig.1|Sakmarian|Sakmarian|Geological Province: Carnarvon Basin.||||||
27365|Carrandibby Formation|60386|6|Mentioned|p297|Sakmarian|Sakmarian|Carnarvon Basin. Proximal shelf.||||||
27365|Carrandibby Formation|61958|5|Briefly described|Map sheet 1|||Age is Artinskian or Sakmarian.||||||
27365|Carrandibby Formation|63469|5|Briefly described|map legend|Permian|Carboniferous|Of Lyons Group.||||||24-SEP-07
27365|Carrandibby Formation|64630|5|Briefly described|p31 Fig.2|Sakmarian|Sakmarian|Province: Southern Carnarvon Basin. Uppermost part of Lyons Group. Underlies the Callytharra Formation. Palynology age: P. pseudoreticulata. Correlates to Holmwood Shale.||||||18-JAN-10
27365|Carrandibby Formation|64974|6|Mentioned|p147 Fig. 5|Sakmarian|Sakmarian|Geological Province: Carnarvon Basin.||||||24-JUN-09
27365|Carrandibby Formation|66579|5|Briefly described|Map legend|Permian|Carboniferous|Southern Carnarvon Basin.||Unit in Lyons Group.|||Grey-green shale and siltstone, coarsening and more calcareous upwards; local dropstones.|
27365|Carrandibby Formation|67200|5|Briefly described|p7 fig 5,|Permian|Permian|||Lyons Group||Overlain by Callytharra Formation|Crudely bedded tillite and siltstone with invertebrate macrofossils.|
27365|Carrandibby Formation|69166|4|Described|geologyp_lut.csv|Sakmarian|Sakmarian|||Lyons Group|||Grey-green shale and siltstone, coarsening and more calcareous upwards; local dropstones|
27365|Carrandibby Formation|69547|6|Mentioned|p182,193,198|Sakmarian|Sakmarian|Southern Carnarvon Basin.|||Unit of Lyons Group.|||
27365|Carrandibby Formation|70774|5|Briefly described|p5 fig 3|Sakmarian|Sakmarian|Southern Carnarvon Basin.||||Overlies the Lyons Group. Overlain by the Callytharra Formation.||
27365|Carrandibby Formation|70795|4|Described|100k_geologyp_lut.csv|Sakmarian|Sakmarian|Also 100k_interpgeop_lut.csv|295-290 Ma||||Grey-green shale and siltstone, coarsening and more calcareous upwards; local dropstones.|
27365|Carrandibby Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||claystone, siltstone, shale, sandstone|
27365|Carrandibby Formation|72910|5|Briefly described|p20-21.|Sakmarian|Sakmarian|Referred to in previous literature (Hocking et al. 1987). Outcrop restricted to Byro Sub-basin and an area east of Pels Range. Difficult to differentiate from Callytharra Formation in drill core. Not recognised herein (subsurface).||Lyons Group||Overlies the Harris Sandstone.|Limestone containing glacial deposits (dropstones).|18-FEB-21
75844|Carrarang Sand|69558|4|Described|p27, p30 fig 39, p31 fig 40-41, p113|Early Holocene|Late Pleistocene|Edel Land Peninsula, Shark Bay. Named for the Carrarang Station. More than 10m thick. See also p33 fig 44, p62 fig 90, p63 fig 91-92, p64, p95.|||||Pale-red and yellow to white, medium-grained, weakly lithified, calcareous sands made up of fragments of molluscs, foraminifers and quartz sand. This sand variably forms Seif, parabolic, barchan and undulating dunes.|24-MAY-21
34374|Carrawine Supersequence|22682|5|Briefly described|Fig20,p29|Archean|Archean|2590-2543 Ma. Hamersley Province. See also Brockman Supersequence||||||03-MAR-10
41811|Carrington Suite|7821|5|Briefly described|p45|||Arunta Inlier.|1779 +/- 6 Ma.||||Granites.|
41811|Carrington Suite|50369|5|Briefly described|p1.3, 6.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Age: 1780Ma.||||||07-NOV-08
41811|Carrington Suite|62633|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Granite, various unnamed divisions within suite.||||||07-NOV-08
41811|Carrington Suite|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Undivided; weakly porphyritic to equigranular biotite granite.||||||
41811|Carrington Suite|64677|6|Mentioned|p31||||c.1770 Ma (Young et al., 1995).|||||
41811|Carrington Suite|65329|6|Mentioned|Map legend|Palaeoproterozoic|Palaeoproterozoic|Abbreviation of Carrington Granite Suite||||||
41811|Carrington Suite|65330|6|Mentioned|Map legend|Palaeoproterozoic|Palaeoproterozoic|Abbreviation of Carrington Granite Suite||||||
41811|Carrington Suite|65332|5|Briefly described|Map Legend|Palaeoproterozoic|Palaeoproterozoic|Informally subdivided in to 7 unnamed granite bodies. Varies from fine-, medium-, to coarse-grained, equigranular to porphyritic granodiorite and granite. Shown as equivalent age to Rapide Granite, older than 1770-1760Ma Yambah Event, younger than Reynolds Range Group, Nicker beds.||||||09-OCT-18
41811|Carrington Suite|68994|4|Described|p4, p6, p8||||c. 1805-1770 Ma magmatic age, Edgoose et al. 2008.||Dwarf Well Granite|Intrudes Lander Rock Formation. Dwarf Well Granite is overlain by Lake Mackay Quartzite.|Granitic rocks.|
41811|Carrington Suite|69003|5|Briefly described|p5, p31|Paleoproterozoic|Paleoproterozoic|West Arunta Orogen. Intrusion coincides with the Yambah Event.|1805-1770 Ma.|||Is overlain by Lake McKay Quartzite. Intrudes Lander Rock Formation.|Metagranitic rocks.|
41811|Carrington Suite|69031|5|Briefly described|p4,p6, p17-22, p24, p26,p43,p47,p59,p67|Statherian|Orosirian|Aileron Province, Arunta Orogen. Gravity, magnetic maps. Uranium-rich: distance to this unit was used as a predictor in modelling for U sources.|1805-1770 Ma.||Dwarf Well Granite.|Intrudes Lander Rock Formation.|Granitic rocks.|
41811|Carrington Suite|69417|5|Briefly described|p2:5|Statherian|Statherian|Aileron Province.|1780-1760 Ma.|||||12-JUL-16
41811|Carrington Suite|69427|5|Briefly described|p12:3, 30, 33|Statherian|Statherian|Young et al. (1995). Aileron Province. Included most foliated biotite-rich granitic rocks in MOUNT DOREEN map area, N and S of the Ngalia Basin. SHRIMP U-Pb zircon age. Other ages range from c.1773 Ma to c.1767 Ma.|1779 +/- 7 Ma (Young et al., 1995).|||Intrudes Reynolds Range Group.|Biotite tonalite to biotite-muscovite granite; most commonly equigranular and medium-grained, although porphyritic varieties also occur. Local andalusite-bearing granite; some merging into migmatite: may be S-type.|12-JUL-16
41811|Carrington Suite|69508|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province. Four un-named subunits are mapped separately. LITHOLOGY (continued): Contains aplite and leucocratic veins and rare clots of radial tourmaline; rare cordierite- and garnet-bearing phase.|||Rapide Granite.||Porphyritic to equigranular biotite granite, commonly biotite-rich, varies from fine- to coarse-grained, leucocratic in places; lesser muscovite granite; biotite-hornblende granite; ubiquitously foliated. See COMMENTS for more.|
41811|Carrington Suite|70762|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Orogen, North Australian Craton.|1779-1767 Ma.||Dwarf Well Granite.|Is overlain by Lake MacKay Quartzite.|Coarse-grained biotite metamonzogranite; granite gneiss interlayered with metagabbro.|
41811|Carrington Suite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
41811|Carrington Suite|71839|6|Mentioned|p10||||1820-1760 Ma||||Felsic intrusions.|22-MAR-23
41811|Carrington Suite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Orogen.|Max age 1779+/-7 Ma, min 1767+/-4 Ma.||Includes Dwarf Well Granite, Rapide Granite.||Weakly porphyritic to equigranular biotite metagranite.|
41811|Carrington Suite|72366|5|Briefly described|p7|Statherian|Statherian|Geological province: Aileron Province. Represents second phase (second of three) of felsic magmatism in the MOUNT DOREEN map sheet, as indicated by a biotite granite with 1779+\-7 Ma magmatic crystallisation age (Young et al., 1995).|c. 178-.176 Ga||||Biotite granite.|08-JAN-20
41811|Carrington Suite|72376|5|Briefly described|p1|Paleoproterozoic|Paleoproterozoic|Geological province: Aileron Province. Outcrops ~7km SW of Wilfram Hill tungsten-copper deposit (Young et al., 1996). A biotite granite of the suite near the Mount Hardy deposit has a U-Pb zircon magmatic crystallisation age of 1779+\-7 Ma (Young et al., 1995).|||||Biotite granodiorite, biotite tonalite, and muscovite-biotite granite.|
79242|Carynginia Sequence|69297|6|Mentioned|p204, p209, p223, p225, p234, p236, p238|||Perth Basin. ||||Overlies the Irwin River Sequence.||
79242|Carynginia Sequence|70097|6|Mentioned|p4|||In the Middle to Late Permian, was partly or totally removed by erosion from the Beagle Ridge and parts of the Abrolhos Sub-basin.||||||30-SEP-16
23475|Cascade Bay Monzogranite|23722|4|Described|p13|Proterozoic|Proterozoic|Geological Province: Hooper Complex||||||
23475|Cascade Bay Monzogranite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1860Ma. Geological province: Kimberley Province (West).||||||07-FEB-11
23475|Cascade Bay Monzogranite|42814|5|Briefly described|p9|||||||||
23475|Cascade Bay Monzogranite|42815|5|Briefly described|map|||||||||
23475|Cascade Bay Monzogranite|43281|5|Briefly described|Map legend||Proterozoic|||||||
23475|Cascade Bay Monzogranite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Paperbark Supersuite.||||||07-NOV-08
23475|Cascade Bay Monzogranite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Paperbark Supersuite.|||Foliated coarsely porphyritic biotite muscovite monzogranite with coarse K-feldspar phenocrysts and recrystallised biotite and quartz defining a strong tectonic foliation|
33874|Cashmans Metasediment|22534|6|Mentioned|Fig.8 p18|||||||||
33874|Cashmans Metasediment|65834|6|Mentioned|p39|||Appears (in very small print) as the informal Cashmans metasediment.||||||
31877|Cassandra Member|23602|4|Described|p11|||See also p6 Table 1. Of Yandagooge Formation. Overlying unit Butler Creek Formation. Max. thickness: <230 m.||||||
31877|Cassandra Member|43848|5|Briefly described|Map Legend||Proterozoic|of Yandagooge Formation.||||||
31877|Cassandra Member|50436|5|Briefly described|p2.1|||Of the Yandagooge Formation.||||||
31877|Cassandra Member|64943|4|Described|p10 Table 2|Paleoproterozoic|Paleoproterozoic|<230 m; iron-rich graphitic, pelitic schist, BIF and chert; member in upper part of Yandagooge Formation, Talbot Terrane, Rudall Complex. Type locality given. Conformable contact with overlying Butler Creek Formation?||||||
27737|Cassidy Group|22816|5|Briefly described|p10 Fig. 4|Mesoproterozoic|Mesoproterozoic|Central Officer Basin||||||
27737|Cassidy Group|30385|6|Mentioned|p8|||||||||
27737|Cassidy Group|30388|4|Described|Table 1|||Middle Proterozoic age||||||
27737|Cassidy Group|30390|4|Described|p57|||See also P58||||||10-JUL-13
27737|Cassidy Group|30884|6|Mentioned|p159|||Comparison of chemical analyses.||||||
27737|Cassidy Group|30944|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27737|Cassidy Group|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27737|Cassidy Group|36551|6|Mentioned|Table 31|||||||||
27737|Cassidy Group|36701|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27737|Cassidy Group|36886|4|Described|p197|||||||||
27737|Cassidy Group|37707|6|Mentioned|p24|||||||||
27737|Cassidy Group|40089|6|Mentioned|Table 29|||||||||
27737|Cassidy Group|44139|5|Briefly described|p284, Table 3-16|||Of Bentley Supergroup.  ~3500m. Basalt, rhyolite, rhyodacite. | | ||||10-SEP-12
27737|Cassidy Group|45149|5|Briefly described|p19|||||||||
27737|Cassidy Group|50607|5|Briefly described|p3.2|||Geological Province: Musgrave Block. Of the Bentley Supergroup.||||||
27737|Cassidy Group|62453|6|Mentioned|p15|||Of the Bentley Supergroup.||||||
27737|Cassidy Group|63866|5|Briefly described|p202|||Musgrave Province.||Bentley Supergroup||||
27737|Cassidy Group|64580|4|Described|map legend||Mesoproterozoic|Of Bentley Supergroup.  Rhyolite and basalt; minor sandstone and siltstone.||||||09-DEC-08
27737|Cassidy Group|64725|6|Mentioned|p64.|||||Unit in Bentley Supergroup.||||
27737|Cassidy Group|65102|6|Mentioned|p363, Figure 4-38, p364|Mesoproterozoic|Mesoproterozoic|Paterson Orogen (SE). Of Bentley Supergroup. Underlies Officer Basin.||||||
27737|Cassidy Group|65410|6|Mentioned|p73 Fig.2.|Proterozoic|Proterozoic|Western Officer Basin.||||||
27737|Cassidy Group|65416|6|Mentioned|p137 Fig.2.|Mesoproterozoic|Mesoproterozoic|Western Officer Basin.||||||
27737|Cassidy Group|67244|5|Briefly described|Map legend.|||Bentley Basin. Shown only in the Interpreted Bedrock Geology section of the map sheet.||Unit in Bentley Supergroup.|Includes Wururu Rhyolite and Gurgadi Basalt.|||11-APR-12
27737|Cassidy Group|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bimodal volcanic rocks.|<1065 Ma.|Unit in Bentley Supergroup.|Includes Wururu Rhyolite and Gurgadi Basalt.|||02-DEC-13
27737|Cassidy Group|67375|5|Briefly described|p7 Fig.4, p16 Fig.10, p38 Table 1. |Mesoproterozoic|Mesoproterozoic|Talbot Sub-basin, Musgrave Region.|||Includes Wururu, Gombugurra, Thomas and Hilda Rhyolites; Gurgadi, Warubuyu and Miller Basalts.|Overlies Pussy Cat Group. Is overlain conformably by Mission Group.|A bimodal volcanic sequence with minor volcanosedimentary rocks.|
27737|Cassidy Group|67553|4|Described|p8,17,40-42,44,51-54,59,94|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Talbot Sub-basin, Bentley Sub-basin. Thickness: slightly over 3000m. Alternating sequence of rhyolitic and basaltic lava flows, with minor intercalations of sedimentary rocks. Rhyolitic units range between 260-550m thick and are dark-grey, feldspar-phyric rhyolites with a very fine grained groundmass, and all can be massive, flow banded, or spherulitic (Daniels, 1974).||Unit of Bentley Supergroup.|Incldues Miller Basalt, Hilda Rhyolite, Warubuyu Basalt, Thomas Rhyolite, Gurgadi Basalt, Gombugurra Rhyolite and Wururu Rhyolite.|Overlain by Mission Group/Gamminah Conglomerate. Conformably underlain by Pussy Cat Group/Glyde Formation.||06-AUG-19
27737|Cassidy Group|68995|5|Briefly described|p3-p4, p7-9, p14-15, p18, p22, p24|Stenian|Stenian|Talbot Sub-basin. Age based on the Giles Event which occurred as this unit was deposited. Over 3400m thick. Geochemistry discussed. See also p43, p45-46, p57.|c. 1085-1040 Ma|Bentley Supergroup|Wururu Rhyolite, Gombugurra Rhyolite, Gurgadi Basalt, Thomas Rhyolite, Warubuyu Basalt, Hilda Rhyolite, Miller Basalt|Overlies the Pussy Cat Group or the Kaarnka Group. Conformably overlain by the Mission Group.|Bimodal succession of rhyolitic lavas or lava-like rheomorphic ignimbrites alternating with basaltic lava flows and minor intercalations of sedimentary rocks.|
27737|Cassidy Group|68996|5|Briefly described|p5, 7, 32, 36, 47, 50, 52 , 59, 68|Mesoproterozoic|Mesoproterozoic|Age of Cassidy and Mission Groups given as 1065-1050 Ma. Essentially undeformed.||Bentley Supergroup|||Mainly intercalated basalt and rhyolites.|
27737|Cassidy Group|69003|5|Briefly described|p37, p51-52|Mesoproterozoic|Mesoproterozoic|Talbot Sub-basin, west Musgrave Province. c.3000m thick.|1065 +/- 5 Ma - 1057 +/- 6 Ma.|Bentley Supergroup.||Overlies Pussy Cat Group, probably unconformably. Is overlain conformably by Mission Group.|Succession of alternating rhyolitic and basaltic units.|
27737|Cassidy Group|69091|4|Described|p30 Fig.3.5, p41 Fig.3.8, see comments|||Talbot Sub-basin, Musgrave Province. Four major mafic-felsic volcanic cycles, combined thickness: >3400 m. Very unusual size (extent and volume) and facies associations. Outcrops with very well developed and continuous flow-banding (in highly felsic rocks), including extensive evidence for rheomorphism, and high-temperature contact metamorphic assemblages in interflow sedimentary units. Misspelled as Cassidy group in p119 Fig.5.16. See also p52 Fig.4.1, p54 Fig.4.2, p59 Fig.4.6, p71 Fig.4.14, p75, p81 Fig.4.17, p106-109, p114, p115 Fig.5.14, p117 Fig.5.15, p119 Fig.5.16, p131 Fig.6.1, p133-134 Fig.6.2, p144-145, p174 Fig.9.5, p177 Fig.9.6, p200 Fig.10.2.||Bentley Supergroup|Miller, Warubuyu, Gurgadi Basalts; Hilda, Thomas, Gombugurra and Wururu Rhyolites.|Is conformably overlain by Mission Group.|Magma compositions are water-poor but F-, alkali- and FeO-rich, and reflect very high eruptive temperatures (>900 degrees C).|
27737|Cassidy Group|69153|5|Briefly described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen. Mentioned in GEOCHRON/174691.1.pdf and 174690.1.pdf.||Bentley Supergroup|Miller Basalt, Hilda Rhyolite, Wururu Rhyolite, Gombugurra Rhyolite, Thomas Rhyolite, Gurgadi Basalt, Warubuyu Basalt||Succession of alternating rhyolitic and basaltic lava flows with minor intercalations of sedimentary rocks; massive to vesicular and amygdaloidal basalt and porphyritic rhyolite; locally common volcanolithic conglomerate and sandstone|
27737|Cassidy Group|69655|5|Briefly described|p3, p6|Stenian|Stenian|Musgrave Region.|c. 1090-1040 Ma|Bentley Supergroup||||
27737|Cassidy Group|69729|5|Briefly described|p66 Fig.1, p68, p70, p80, p82|||Talbot Sub-basin, Musgrave Province.||Bentley Supergroup.|Wururu, Gombugurra, Thomas, Hilda Rhyolites; Gurgadi, Warubuyu, Miller Basalts.|Overlies the Pussy Cat Group. Is overlain conformably by the Mission Group.||
27737|Cassidy Group|70095|5|Briefly described|p16-18|||Geological province: Musgrave Province. Talbot Sub-basin, Of Bentley Basin. Bimodal volcanic cycles that form the entire upper half of the extrusive sequence and are continuous over strike lengths  of over 90km. Youngest volcanism associated with the Kaarnka caldera cluster; starting with highly 18O-depleted (Wururu Rhyolite) progressively trending to less 18O-depleted (Thomas Rhyolite) rhyolites.||Unit of Bentley Supergroup.|Includes Hilda Rhyolite, Miller Basalt, Warubuyu Basalt, Thomas Rhyolite, Gurgadi Basalt, Gombugurra Rhyolite and Wururu Rhyolite.|Overlain by Mission Group. Underlain by Pussy Cat Group.||
27737|Cassidy Group|70134|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Bentley Supergroup.|Wururu, Gombugurra, Thomas Rhyolites.|Overlies Pussy Cat Group.||
27737|Cassidy Group|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Bentley Supergroup.|Wururu, Gombugurra, Thomas, Hilda Rhyolites; Gurgadi [mis-spelling of Gurgadi], Warubuyu, Miller Basalts.||Rhyolites, basalts; sandstone, siltstone and mudstone.|12-NOV-15
27737|Cassidy Group|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic||1047 Ma - 1077 Ma (Inferred)|Bentley Supergroup|Includes Gurgadi Basalt, Hilda Rhyolite, Miller Basalt, Gombugurra Rhyolite, Thomas Rhyolite, Wururu Rhyolite, Warubuyu Basalt,||Fine-grained, thinly interbedded, feldspar-rich volcaniclastic sandstone, siltstone and volcanolithic conglomerate; Massive-vesicular and amygdaloidal basalt and porphyritic rhyolite.|
27737|Cassidy Group|70793|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv.|1077-1047 Ma (inferred)|Unit of Bentley Supergroup.|Includes Gombugurra Rhyolite, Gurgadi Basalt, Hilda Rhyolite, Miller Basalt, Thomas Rhyolite, Warubuyu Basalt, Wururu Rhyolite.||Massive to vesicular and amygdaloidal basalt and porphyritic rhyolite; locally common volcanolithic conglomerate and sandstone|
27737|Cassidy Group|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Bentley Basin. ||Bentley Supergroup||||
27737|Cassidy Group|70831|5|Briefly described|p3|||Musgrave Province.||Bentley Supergroup||||
27737|Cassidy Group|71170|5|Briefly described|p5|||Talbot Sub-basin. Emplaced during the Giles Event.||||||
27737|Cassidy Group|71210|6|Mentioned|p5|||Talbot Sub-basin.||||||
27737|Cassidy Group|71211|6|Mentioned|p6 fig 1.3, p7 fig 1.4, p12, p24 fig 2.1|||See also p25, p26, p27 fig 2.3, p84 fig 3.1, p86, p87 fig 3.2, p136 fig 4.1, p137 fig 4.2, p216, p234. ||Bentley Supergroup|Includes the Miller Basalt, Hilda Rhyolite, Warubuyu Basalt, Thomas Rhyolite, Gurgadi Basalt, Gombugurra Rhyolite and the Wururu Rhyolite.|Overlies the Pussy Cat Group. Conformably overlain by the Mission Group.||
27737|Cassidy Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||acid and basic volcanic rock|
27737|Cassidy Group|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Represents a succession of alternating rhyolitic (Wururu, Gombugurra, Thomas, and Hilda Rhyolites) and basaltic (Gurgadi, Warubuyu, and Miller Basalts) lava flows. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv.|1077-1047 Ma (inferred)|Unit of Bentley Supergroup.|Includes Gombugurra Rhyolite, Gurgadi Basalt, Hilda Rhyolite, Miller Basalt, Thomas Rhyolite, Warubuyu Basalt, Wururu Rhyolite.||Alternating massive to vesicular and amygdaloidal basalt and porphyritic rhyolite; interlayered with fine-grained, thinly interbedded, feldspar-rich volcaniclastic sandstone and siltstone; locally common volcanolithic conglomerate.|
27737|Cassidy Group|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Bentley Supergroup|||Massive to vesicular and amygdaloidal basalt and porphyritic rhyolite; locally common volcanolithic conglomerate and sandstone.|
27737|Cassidy Group|72094|4|Described|p3 Fig 2, p4, 6, 13|Mesoproterozoic|Mesoproterozoic|Talbot Sub-basin, Bentley Basin.||Unit of Bentley Supergroup.|||Massive, vesicular and amygdaloidal basalt and porphyritic rhyolite with locally common volcanogenic conglomerate and sandstone.|
27737|Cassidy Group|72443|4|Described|p737-741, p747-748, p753, p756, p760|||Talbot Sub-basin. Dips shallowly to the south and SW and form continuous packages that can be traced for over 100km. Maximum thickness of >3km. Geochemistry and petrology are discussed.||Bentley Supergroup|Includes the Wururu Rhyolite, Gombugurra Rhyolite, Gurgadi Basalt, Thomas Rhyolite, Warubuyu Basalt, Hilda Rhyolite and the Miller Basalt.|Overlies the Pussy Cat Group. Conformably overlain by the Mission Group.|Rhyolitic lavas or lava-like rhepomorphic ignimbrites and basalt flows. Rhyolites are typically dark grey and feldspar-phyric with a very fine-grained groundmass and can be massive, flow[banded or spherulitic.|
27737|Cassidy Group|73437|6|Mentioned|p151|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Talbot Sub-basin.||Bentley Supergroup||||
79243|Cattamarra Sequence|69297|5|Briefly described|p202, p204, p206|Middle Jurassic|Early Jurassic|Perth Basin. Exhibits good organic richness and potential to generate gas. See also p207, p209, p223, p225, p236, p238.||||Overlies the Eneabba Sequence. Overlain by the Cadda Sequence.|Interbedded sandstone, siltstones and coals.|
79243|Cattamarra Sequence|70097|5|Briefly described|p4|Middle Jurassic|Early Jurassic|Houtman Sub-basin.||||||20-OCT-15
31024|Cattle Well Formation|23046|5|Briefly described|174|||||||||
31024|Cattle Well Formation|23415|5|Briefly described|Map Legend|Archean|Archean|Of De Grey Group. Geological province: Pilbara Craton. Interbedded dacite tuff, welded tuff and tuffaceous siltstone and shale, and thin-bedded sandstone, siltstone, wacke, and carbonate rock; weakly metamorphosed.||||||07-NOV-08
31024|Cattle Well Formation|23757|4|Described|p12|Archean|Archean|Age: <3048 Ma (SHRIMP U-Pb zircon). Of De Grey Group. Disconformable over Cooieena Basalt; unconformable below Callawa Fm. Interbedded metamorphosed wacke, sandstone and siltstone. Intruded by quartz gabbro, prob. part of layered mafic Shay Intrusion||||||07-NOV-08
31024|Cattle Well Formation|23783|5|Briefly described|p17||Archean|Of De Grey Group.||||||07-NOV-08
31024|Cattle Well Formation|23955|4|Described|p1241 Fig. 2, p1242 Fig.3|||Overlies the Scuddles Formation. Maximum Thickness: 1450m. Geological Province: Murchison province, Yilgarn Craton.||||||
31024|Cattle Well Formation|24025|4|Described|p8 Tb. 1|Archean|Archean|Of De Grey Group.  Max. thickness: ~2500m.  Thinly bedded sandstone, feldspathic sandstone and wacke; interbeds of siltstone and shale.  Geological Province: Pilbara Craton.||||||22-NOV-16
31024|Cattle Well Formation|24110|5|Briefly described|Plate 1|Archean|Archean|Of the De Grey Group. Geological Province: Pilbara Craton.||||||07-NOV-08
31024|Cattle Well Formation|24184|5|Briefly described|p703, p699 Fig.3|Archean|Archean|Parent: De Grey Group. Underlying Unit: Cooeenia Basalt. Geological Province: Pilbara Craton. Age: ca.3048Ma||||||07-NOV-08
31024|Cattle Well Formation|24531|5|Briefly described|p5 Tb. 1|Archean|Archean|Of the De Grey Group (Pilbara Supergroup).  Age: </-c.3048Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
31024|Cattle Well Formation|44229|5|Briefly described|Map Legend|Archean|Archean|Of the De Grey Group.  Interbedded dacit tuff, welded tuff, tuffaceous siltstone and shale, and thin-bedded sandstone, siltstone, wacke, and carbonate rocks.||||||07-NOV-08
31024|Cattle Well Formation|50189|4|Described|p18|Archean|Archean|Of the De Grey Group; together with the Cooragoora Formation, replacing the Lalla Rookh Sandstone. Dacite tuff. Overlain by Cooieena Basalt; unconformably overlain by Eel Creek Formation; overlies Cooiena Basalt. Age: 3555 +/- 3Ma - 3048 +/- 19Ma.||||||07-NOV-08
31024|Cattle Well Formation|50544|3|Fully described|p34, p19 Tb. 2 (amended)|Archean|Archean|Of the De Grey Group.  Conformably overlain by Cooragoora Formation; overlies Cooieena Basalt (Gorge Creek Group).  Max. age: 3048+/-19Ma.  Max. thickness: ~2500m.  See also p21 Tb. 4||||||07-NOV-08
31024|Cattle Well Formation|50555|5|Briefly described|Map legend|Archean|Archean|Of the De Grey Group (Pilbara Supergroup).  Interbedded dacite tuff, welded tuff, tuffaceous siltstone and shale, and thin-bedded sandstone, siltstone, wacke and carbonate rock; silicified stromatolites.   Age: <3048Ma. Geol. Province: Pilbara Craton.||||||07-NOV-08
31024|Cattle Well Formation|60429|4|Described|p18, p37 Appx. 1|Archean|Archean|Of De Grey Gp. Together with Cooragoora Fm, previously mapped as Lalla Rookh Sst. Disconformable on Cooieena Basalt; unconformably overlain by Eel Creek Fm. Age: 3048+/-19Ma (dacite tuff, Nelson, in prep).Max. thickness: 2500m. Detailed lithology incl.||||||07-FEB-11
31024|Cattle Well Formation|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Geological Province: eastern Pilbara Craton.||||||07-NOV-08
31024|Cattle Well Formation|63441|5|Briefly described|p5 Tb.1, p29|Archean|Archean|Of Croydon Group (Pilbara Supergroup). Max. thickness: 2600m. Geol. prov: Mallina Basin, Pilbara Craton. Siltstone, sandstone and wacke, with local interbeds of rhyolite flows, felsic volcaniclastic rocks and silicified evaporites, including carbonates.||||||07-FEB-11
31024|Cattle Well Formation|63538|4|Described|p6 Fig. 3|Archean|Archean|Of Croydon Group. Underlain by Bookingarra Formation. Geological Province: Pilbara Craton. Felsic volcanic rocks.||||||19-APR-13
31024|Cattle Well Formation|66217|6|Mentioned|p39.|||||Unit in Croydon Group.|||Felsic volcanics.|
31024|Cattle Well Formation|67201|4|Described|p7 Fig.4, p12 Tb.1, p21 Fig.12|||In northwestern Pilbara Craton, East Pilbara Terrane, De Grey Superbasin, Mallina Basin.|c. 2980 Ma|Croydon Group||||
31024|Cattle Well Formation|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|Age derived from sample of felsic volcanic rock and felsic volcanic tuff  (180048.1.pdf, 142867.1.pdf) wherein it constrains the age of the volcanic components crystallization.|2988 +/- 5 Ma -3048 Ma +/- 19 Ma (SHRIMP)|Croydon Group|||Sandstone, siltstone, shale, and wacke; minor felsic volcaniclastic rocks; local chert replacing stromatolitic carbonate rocks; metamorphosed|
31024|Cattle Well Formation|69185|5|Briefly described|500k_interpgeop_pilcrat02_lut.csv||Archean|Geological province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton. Of Budjan, Cattle Well, Goldsworthy, Lalla Rookh, and Mosquito Creek Basins.||||||
31024|Cattle Well Formation|69301|4|Described|p5 Fig.3, p9 Tb.1, p15, p20 Tb.2, p22|||Pilbara Craton. East Pilbara Terrane. Mallina Basin. Age: ca 2.99 Ga U-Pb zircon age obtained for volcaniclastic sandstone - zircons could be inherited.|2980 Ma, see comments.|Croydon Group||Is overlain by Lalla Rookh Sandstone. Overlies Coonieena Basalt.|Felsic volcaniclastic rocks. Silicified carbonate and evaporite rocks contain stromatolite-like structures.|
31024|Cattle Well Formation|69590|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton. Of Lalla Rookh Basin, De Grey Superbasin. Events: North Pilbara Orogeny. Sample GSWA 142867 (felsic tuffaceous unit) yielded an interpreted maximum depositional age of 3048+\-19 Ma for the tuffaceous unit (weighted mean 207Pb/206Pb). Sample GSWA 180048 (felsic volcanic) yielded an interpreted maximum depositional age of 2988+\-5 Ma (weighted mean 207Pb/206Pb), which may also be alternatively interpreted as maxmimum age of deposition for the volcanic precursor. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|2988-2940 Ma (isotopic; inferred)|Unit of Croydon Group.|||Sandstone, siltstone, shale, and wacke; minor felsic volcaniclastic rocks; local chert replacing stromatolitic carbonate rocks; metamorphosed|
31024|Cattle Well Formation|70020|4|Described|p131|||Geological province: Yilgarn Craton; central Yalgoo-Singleton greenstone belt. Thickness: 900-1400m.||Unit of Gossan Hill Group.||Overlain by Thundelarra Group. Underlain by Scuddles Formation.|Polymict sandstone and minor basalt.|
31024|Cattle Well Formation|70022|6|Mentioned|p115|||East Pilbara Terrane.||Croydon Group.||||
31024|Cattle Well Formation|70270|5|Briefly described|p519 Fig. 2, p520 Fig. 3|||Murchison Province. 900-1400m thick.||Of Gossan Hill Group||Shown as overlying Scuddles Formation.|Polymict sandstone and minor basalt|26-JUN-18
31024|Cattle Well Formation|70775|5|Briefly described|iv, p12, p55, p81|||There is a potential correlation between this formation and felsic volcanic rocks of the Whim Creek Group in the east Pilbara.|c. 2988 Ma|Croydon Group||Overlies the Mallina Formation (lower). Overlain by the Lalla Rookh Sandstone. Unconformably overlain by the Cistern Formation.||
31024|Cattle Well Formation|71168|4|Described|p11, p12 fig 6, p13 fig 7, p57|||Yilgarn Craton. Appears as the Cattle Well formation on p11. Thickness ranges from 900-1400m.||Gossan Hill Group||Overlies the Scuddles Formation.|Polymict sandstone and minor basalt.|
31024|Cattle Well Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mallina Basin.|2988 +/-5 Ma.|Croydon Group|||Sandstone, siltstone, shale, and wacke; minor felsic volcaniclastic rocks; local chert replacing stromatolitic carbonate rocks; metamorphosed.|
31024|Cattle Well Formation|72251|5|Briefly described|p54|Mesoarchean|Mesoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Croydon Group.||Overlain by Lalla Rookh Sandstone. Underlain by Coonieena Basalt.||
31024|Cattle Well Formation|72668|5|Briefly described|p4, p15|||East Pilbara Terrane. 1500 m thick. Preliminary zircon data from a rhyolite at the base of the Cattle Well Formation indicates a depositional age of c. 2990 Ma.||Croydon Group||Overlies the Bookingarra Formation. Overlain by the Constantine Sandstone and the Lalla Rookh Sandstone.|Fine-grained sedimentary rocks, rhyolite and associated felsic volcaniclastic rocks.|12-JAN-22
31024|Cattle Well Formation|73598|6|Mentioned|p1212|Mesoarchean|Mesoarchean|East Pilbara Terrane.||Croydon Group.||Overlies Coonieena Basalt. Is overlain by Lalla Rookh Sandstone.||
79372|Cave Hill Member|72712|5|Briefly described|p12, 14, 15,16, 17, 43,44, 47, 55, 57.|Siderian|Siderian|New name. Lith description for Hardey Syncline where it si 55 m thick. Glacigenic component is thicker in original discovery site in Duck Creek Syncline, and includes rhyolite dropstones. Age constrained by Boolgeeda Iron Formation MDA and 2444+/-3 Ma age for underlying Woongarra Rhyolite.|< 2454 +/- 23 Ma.|Top of Boolgeeda Iron Formation.||Top of Boolgeeda Iron Formation and unconformably underlies Kungarra Formation.|Mostly BIF, silty BIF and jaspilite. Includes minor sandstone/diamictite at base, overlain by siltstone and mudstone.|
81582|Cave Rocks Dolerite|72057|4|Described|p237-239,241-243,247,248, 250|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton. Contact with Black Flag Group host sediments is irregular, indicating emplacement into unconsolidated sediments and at relatively shallow depths. Interpreted as an intrusive sill, based on common coarse (>3mm) groundmass grain size, thin hosting sediments indicating relatively flat paleo-depositional enviroment (thus not conducive for lava ponding) and extensive sheet-like geometry. |c. 2680 Ma|Unit of Black Flag Group.|Includes East, West and Beverly dolerites.|||03-SEP-19
81583|Cave Rocks East Dolerite|72057|5|Briefly described|p242,244,245|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton. Thickness: 132-250m, averaging 180m. Sharp contact with Black Flag Group. West-facing, consistent with overall stratigraphy of the host sequence. Also abbreviated to East Dolerite p244.||Unit of Cave Rocks Dolerite.|||Aphyric basalt, grading upward through dolerite and gabbro into pyroxenite, and up into dolerite, minor gabbro and quartz gabbro.|07-FEB-20
28107|Cawse Monzogranite|22534|5|Briefly described|p11|||||||||
28107|Cawse Monzogranite|22539|5|Briefly described|Map legend|Archean|Archean|||||||07-NOV-08
28107|Cawse Monzogranite|42705|5|Briefly described|map legend|Archean||||||||07-NOV-08
28107|Cawse Monzogranite|42988|5|Briefly described|Map Legend|||||||||
28107|Cawse Monzogranite|42989|5|Briefly described|p12|||||||||
28107|Cawse Monzogranite|43101|5|Briefly described|p26|||||||||
28107|Cawse Monzogranite|43214|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
28107|Cawse Monzogranite|43232|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
28107|Cawse Monzogranite|60076|5|Briefly described|p45 App. 1|||[Agmca]   Coarse-grained, equigranular, biotite bearing monzogranite.||||||
28107|Cawse Monzogranite|65204|6|Mentioned|p17 Tbl.2,|Neoarchean||0.4-10mm grains; seriate to porphyritic ||||||
28107|Cawse Monzogranite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Coarse-grained biotite monzogranite, equigranular to porphyritic, locally seriate.||||||07-FEB-11
28107|Cawse Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Coarse-grained biotite monzogranite; equigranular to porphyritic, locally seriate; domal in D2 anticlines; moderate to weak foliation; sheared contacts.|05-AUG-15
28107|Cawse Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Coarse-grained biotite monzogranite; equigranular to porphyritic, locally seriate; domal in D2 anticlines; moderate to weak foliation; sheared contacts.|
28107|Cawse Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
28107|Cawse Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv, 100k_geologysub10_lut.csv.|3010-2600 Ma (inferred)||||Coarse-grained biotite monzogranite; equigranular to porphyritic, locally seriate; moderate to weak foliation; metamorphosed|
31106|Cement Granitic Complex|43478|6|Mentioned|p40|||||||||
31106|Cement Granitic Complex|65147|6|Mentioned|p9 Fig.6|||||||||01-FEB-17
35673|Cemetery Conglomerate|23142|5|Briefly described|p203 Fig.2|||||||||
35673|Cemetery Conglomerate|65834|6|Mentioned|p36|||Kanowna Belle gold mine, Boorara Domain, Kalgoorlie Terrane. Mine terminology.||||Is intruded by Kanowna Belle Porphyry.|A lens of felsic-rich conglomerate.|
75827|Centenary Bore Basalt|66192|6|Mentioned|p550, 551|||In Agnew-Wiluna Greenstone Belt. With Mount Keith Dacite, separates the underlying Mount Keith Ultramafic Unit and the overlying Cliff Ultramafic Unit; their combined thickness varies from 0 to c.800 m.||||||09-MAR-12
75827|Centenary Bore Basalt|70275|5|Briefly described|p471, 480, 483, 496|||The uppermost volcanic unit in the Mt. Keith area, Agnew-Wiluna Belt, Kalgoorlie Terrane, Yilgarn Craton.||||Overlies Mount Keith Dacite. Is overlain by Monument Ultramafic Unit. Encloses Cliffs Ultramafic Unit.|Basalt, intercalated with variably sulfidic, fine-grained sedimentary horizons: shales (many carbonaceous) and cherts interspersed with exhalative massive iron sulfide units.|
75827|Centenary Bore Basalt|70276|6|Mentioned|p784-786|||Agnew-Wiluna greenstone belt, Yilgarn Craton.||||Overlies Mount Keith Dacite. Is overlain by Cliffs ultramafic unit.|High Mg/high Fe basalt sequence of tholeiitic affinity intercalated with carbonaceous shales and pyritic cherts.|
75827|Centenary Bore Basalt|70326|4|Described|p360,364|Neoarchean|Neoarchean|Geological province: Boorara Domain North, Kalgoorlie Terrane, Yilgarn Craton.||||Overlain by Cliffs Ultramafic. Underlain by Mount Keith Ultramafic. Correlable to Never Can Tell, Missouri and Lindsay basalts.|Massive and pillowed high-Mg and high-Fe basalt.|
75827|Centenary Bore Basalt|73596|6|Mentioned|p1152|Neoarchean|Neoarchean|Mount Keith Domain, Agnew-Wiluna Greenstone Belt.|2688 +/- 8 Ma.|||||
69187|Centenary Shale|60514|5|Briefly described|p64, p65, p64 Fig. 5|Archean|Archean|Of the Black Flag Group. Maximum thickness: 10m. Geological Province: Yilgarn Craton. The shale is a carbonaceous sedimentary horizon.||||||07-FEB-11
69187|Centenary Shale|60627|5|Briefly described|p64|||Thickness: typically 1.5 m, up to 10m. Carbonaceous. Of Black Flag Group.||||||
69187|Centenary Shale|70153|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Age of parent unit is 2664 +/- 3 Ma (SHRIMP).|2692 - 2655 Ma (age range inferred).|Black Flag Group.|||Carbonaceous shale; locally discontinuous; typically less than 10 m thick; metamorphosed.|
69187|Centenary Shale|71270|4|Described|100k_interpgeol_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma). |2692-2655 Ma (inferred)|Unit of Black Flag Group.|||Carbonaceous shale; locally discontinuous; typically less than 10 m thick; metamorphosed|
69187|Centenary Shale|72814|5|Briefly described|p201, Fig. 3, p202 Fig. 4, p204, p205|||East of Zuleika Shear, Ora Banda Domain.|||||Carbonaceous pyritic shale.|
69187|Centenary Shale|73391|5|Briefly described|p75, 78, 80, 82, 254, 363, 365|||See also Appendices. Rubicon mine area, Ora Banda Domain.||||Overlies Victorious Basalt (Upper Basalt). Is overlain by White Flag Formation and (also correlated with) Talbot formation.|Carbonaceous mudstone, replaced by disseminated arsenopyrite, pyrrhotite and biotite with extensive quartz-sulphide vein emplacement and chlorite alteration near the veins. Generally 1.5m thick; up to 10m locally.|
79600|Central Desert Dolerite Suite|70762|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|North Australian Craton.|||||Dolerite dyke.|
79600|Central Desert Dolerite Suite|70826|6|Mentioned|p14 tbl 5|Tonian|Tonian|West Arunta region.|975 Ma|||||
79600|Central Desert Dolerite Suite|71080|5|Briefly described|p23|Tonian|Tonian||976 +/- 3 Ma (Wyborn et al., 1998)|||Unconformably overlain by Heavitree Formation.||04-FEB-19
79600|Central Desert Dolerite Suite|72259|6|Mentioned|p10|Tonian|Tonian||976 +/- 3Ma|||||
80948|Chabbledoo Formation|71808|4|Described|p61-p62|Miocene|Cenozoic|Lipple (1994) suggested the regional extent and importance of the Tertiary detritals 1(aplaeovalley infills) as a lithostratigraphic marker warranted the formal definition of this unit. The name is derived from the Aboriginal name for the major hills along the northern limit of the Southern Flank. The proposed type section is along a major creek just north of M Deposit where it cuts an eroded basement syncline. The section extends 500m between the northern basal contact (697 980E/ 7 455 660N) and the southern basal contact (698 300E / 7 455 270N). Additional reference sections are provided.||||informal Hematite Siltstone, Red Ochre Detritals, Superband|Moderately stratified interlayered conglomerate, pebbly conglomerate and coarse sandstone, and massive to pebbly siltstone. Bed thickness varies between 0.1 to 2.5 m.Conglomerate near the base contains some megaclasts.|27-APR-19
23478|Challenger Formation|14227|5|Briefly described|Enclos. 2|Oligocene|Eocene|Presented as Challenger Fm.||||||07-FEB-11
23478|Challenger Formation|24160|5|Briefly described|p94|Eocene|Eocene|Perth Basin.|||||Brown calcareous shale, siltstone.|
23478|Challenger Formation|41751|2|Defined|p7|Late Eocene||Quilty's Late Eocene Unnamed Formation.||||||27-JUL-09
23478|Challenger Formation|43700|5|Briefly described|p19|Oligocene|Eocene|||||||
23478|Challenger Formation|44144|4|Described|p502 Tb.4-21, p518 fig 4-162, p519|Late Eocene|Late Eocene|Type Section: Challenger 1 well 530-597m.  67m thick marine shelf deposits.||||Overlies Kings Park Formation disconformably.|Chalk, calcarenite, chert.|
23478|Challenger Formation|61155|5|Briefly described|p15|Late Eocene|Late Eocene|Age: ~40-37.5Ma. Max. thickness: 70m. Geological Province: Perth Basin.||||||
25840|Champion Bay Group|23279|6|Mentioned|p28|||||||||
25840|Champion Bay Group|23578|5|Briefly described|p7|Jurassic|Jurassic|||||||
25840|Champion Bay Group|23816|5|Briefly described|p243|Bajocian|Bajocian|Geological Province: Perth Basin.||||||
25840|Champion Bay Group|24020|5|Briefly described|p387|||Geological Province: Perth Basin||||||16-MAR-05
25840|Champion Bay Group|24160|6|Mentioned|p94|||Perth Basin.|||||Shale, siltstone, sandstone and limestone.|
25840|Champion Bay Group|30948|6|Mentioned|Map legend|Bajocian|Bajocian|||||||
25840|Champion Bay Group|30963|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
25840|Champion Bay Group|31910|4|Described|p22|||Table 1||||||
25840|Champion Bay Group|32648|6|Mentioned|p32|||Jur.||||||
25840|Champion Bay Group|32649|4|Described|p24|||See also Table 1||||||
25840|Champion Bay Group|33022|6|Mentioned|p259|||||||||
25840|Champion Bay Group|33166|6|Mentioned|Fig.1|||Geol. map||||||
25840|Champion Bay Group|35282|6|Mentioned|Fig.2|||||||||
25840|Champion Bay Group|36257|6|Mentioned|Table 2.1|||||||||
25840|Champion Bay Group|36293|2|Defined|p147|Middle Jurassic|Middle Jurassic|||||||
25840|Champion Bay Group|36890|5|Briefly described|p243|||||||||
25840|Champion Bay Group|41284|5|Briefly described|p90|||||||||
25840|Champion Bay Group|41625|6|Mentioned|p1|||||||||
25840|Champion Bay Group|41729|5|Briefly described|p454|||||||||
25840|Champion Bay Group|43031|6|Mentioned|p17|||||||||
25840|Champion Bay Group|43495|5|Briefly described|11-16|||||||||
25840|Champion Bay Group|43710|6|Mentioned|p6|||||||||
25840|Champion Bay Group|44144|5|Briefly described|p505 Tb.4-21, p514-515|Jurassic|Jurassic|Playford (1959).|||Includes Kojarena and Colalura Sandstones, Newmarracarra Limestone and Bringo Shale.||Shale, siltstone, sandstone, limestone.|
25840|Champion Bay Group|48615|14|Not recorded|Fig.4.|||||||||
25840|Champion Bay Group|60376|6|Mentioned|p16, p21|||Includes; Newmarracarra Limestone.||||||07-FEB-11
25840|Champion Bay Group|61811|5|Briefly described|p3 Fig.2, pp29-31, p33.|Bajocian|Aalenian|Northern Perth Basin. Is laterally equivalent to the Cadda Formation, further to the south. At Bringo, records a short-lived marine transgression within otherwise dominantly fluvial facies. Lower erosional contact is a significant sequence boundary.|||Includes Colalura Sandstone at base, then Bringo Shale, Newmarracarra Limestone, and Kojarena Sandstone at top.|Overlies Chapman Group.||
25840|Champion Bay Group|64635|5|Briefly described|p4 Fig.3, p16  |Bajocian|Aalenian|Best-exposed section is in Bringo rail cutting.|||Includes the Colalura Sandstone, Bringo Shale, Newmarracarra Limestone and Kojarena Sandstone.|Overlies the Chapman Group.||
25840|Champion Bay Group|67340|6|Mentioned|p6|Jurassic|Jurassic|Northern Perth Basin.||||||
25840|Champion Bay Group|68135|5|Briefly described|p52, p52 fig 2b|Bajocian|Aaelenian|Perth Basin. Hosts invertebrate (ammonites) and vertebrate body fossil assemblages.|||Newmarracarra Limestone|Overlies Chapman group, overlain by Yarragadee Formation|Interbedded siltstone and limestone.|14-SEP-17
25840|Champion Bay Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||biocarbonate, shale, sandstone|
27740|Chaneys Granite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1860Ma. Geological province: Kimberley Province (West).||||||07-FEB-11
27740|Chaneys Granite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
27740|Chaneys Granite|30525|6|Mentioned|Map legend|Proterozoic|Proterozoic|Part of Lamboo Complex.||||||14-NOV-06
27740|Chaneys Granite|30533|4|Described|p13|||||||||
27740|Chaneys Granite|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27740|Chaneys Granite|32728|6|Mentioned|Table 4|||||||||
27740|Chaneys Granite|36885|4|Described|p174|||||||||
27740|Chaneys Granite|42710|5|Briefly described|map legend|Proterozoic||||||||
27740|Chaneys Granite|42811|5|Briefly described|p11|||||||||
27740|Chaneys Granite|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|Approx 1865 - 1850 Ma.||||||
27740|Chaneys Granite|44155|4|Described|p242 Tb.3-5|||||Hooper Complex||Intrudes Lerida Granite. Equivalent to Lennard Granite.|Coarse-grained biotite syenogranite, monzogranite, or rarely granodiorite; mostly porphyritic.|
27740|Chaneys Granite|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Foliated biotite monzogranite and granodiorite.  Age: 1865-1850Ma.  In the Hooper Complex and Lamboo Complex (western zone).||||||07-NOV-08
27740|Chaneys Granite|44366|14|Not recorded|p.10||Proterozoic|Part of Lamboo Group. Defintion on Tech.File E/52-5.||||||
27740|Chaneys Granite|44367|14|Not recorded|map legend||Proterozoic|(Reprinted 1971). Unit of Lamboo Complex.||||||
27740|Chaneys Granite|44397|14|Not recorded|p.8, Table 1||Proterozoic|In the Lamboo Complex.||||||14-NOV-06
27740|Chaneys Granite|44398|14|Not recorded|map legend||Proterozoic|||||||
27740|Chaneys Granite|50437|5|Briefly described|p1.5, table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Paperbark Supersuite.||||||07-NOV-08
27740|Chaneys Granite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Paperbark Supersuite.|||Coarse and even grained or commonly foliated to weakly porphyritic biotite granite, monzogranite and granodiorite with small mafic xenoliths; locally sheared|
27740|Chaneys Granite|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen, North Australian Craton.||Paperbark Supersuite.|||Foliated biotite metamonzogranite and metagranodiorite; weakly porphyritic; contains small mafic inclusions,.|
27740|Chaneys Granite|72437|5|Briefly described|p64, p73, p75-76|||Hooper Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Porphyritic monzogranite.|
25841|Chapman Group|23578|5|Briefly described|p7|Jurassic|Jurassic|||||||
25841|Chapman Group|23816|5|Briefly described|p242|Early Jurassic|Early Jurassic|Geological Province: Perth Basin. Includes the Greenough Sandstone and Moonyoonooka Sandstone.||||||
25841|Chapman Group|24160|6|Mentioned|p94|||Perth Basin.||||||
25841|Chapman Group|30948|6|Mentioned|Map legend|Lias|Lias|||||||
25841|Chapman Group|30963|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
25841|Chapman Group|31910|4|Described|p21|||Table 1||||||
25841|Chapman Group|32648|6|Mentioned|p32|||L. Jur.||||||
25841|Chapman Group|32649|4|Described|p24|||Table 1||||||
25841|Chapman Group|33022|6|Mentioned|p259|||||||||
25841|Chapman Group|33166|6|Mentioned|p63|||Refers Arkell & Playford (1954)||||||
25841|Chapman Group|36257|6|Mentioned|Table 2.1|||||||||
25841|Chapman Group|36293|2|Defined|p140|Early Jurassic|Early Jurassic|||||||
25841|Chapman Group|36890|5|Briefly described|p242|||||||||
25841|Chapman Group|37340|6|Mentioned|p164|||||||||
25841|Chapman Group|38998|4|Described|p19|||See P23||||||
25841|Chapman Group|40254|6|Mentioned|Fig.1|||||||||
25841|Chapman Group|40340|5|Briefly described|Table 2|||||||||
25841|Chapman Group|40341|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
25841|Chapman Group|41625|6|Mentioned|p1|||||||||
25841|Chapman Group|43495|5|Briefly described|11-16|||||||||
25841|Chapman Group|44144|6|Mentioned|p506 Tb.4-21, p514, p515 fig 4-155|Early Jurassic|Early Jurassic|Playford (1959).|||Includes Greenough and Moonyoonooka Sandstones.|||
25841|Chapman Group|44307|14|Not recorded|p13|||Basin equivalent of Cockleshell Gully Formation.||||||
25841|Chapman Group|48615|14|Not recorded|Fig.4|||(H50-1).||||||
25841|Chapman Group|48857|14|Not recorded|p.10|||||||||
25841|Chapman Group|61811|5|Briefly described|p3 Fig.2, p20, pp26-29, p33.|Toarcian|Toarcian|Northern Perth Basin. Is laterally equivalent to upper Cattamarra Coal Measures further south in the Basin. Upper erosional contact is a significant sequence boundary.|||Includes (lower) Greenough Sandstone and (upper) Moonyoonooka Sandstone.|Disconformably overlies Kockatea Shale. Is overlain by Champion Bay Group.|Two dominantly sandstone units.|
25841|Chapman Group|64635|5|Briefly described|p4 Fig.3, p16  |Toarcian|Toarcian||||Includes the Greenough Sandstone and the Moonyoonooka Sandstone.|Disconformably overlies Kockatea Shale. Overlain by the Champion Bay Group.|Consists of two dominantly sandstone units.|
25841|Chapman Group|64769|6|Mentioned|p129 Fig. 132|Mesozoic|Jurassic|Sandstone.||||||06-MAY-09
25841|Chapman Group|67340|6|Mentioned|p6|Jurassic|Jurassic|Northern Perth Basin.||||||
25841|Chapman Group|68135|5|Briefly described|p52 fig 2b |Aalenian|Sinemurian|Perth Basin. ||||Overlain by Champion Bay Group|Silty sandstone.|14-SEP-17
25841|Chapman Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone|
31956|Chararoo Granite|24197|6|Mentioned|p71 Tb. 7.1|||Of the Chararoo Supersuite.||||||07-FEB-11
31956|Chararoo Granite|50425|5|Briefly described|p1.3, 3.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Province.  Of the Chararoo Supersuite.||||||07-NOV-08
31955|Chararoo Supersuite|24197|5|Briefly described|p69, p71 Tb. 7.1|Paleoproterozoic|Paleoproterozoic|Parts of this supersuite may be incorporated into the Minnie Creek Supersuite. Includes Chararoo, Pimbyana, Nyang, Joy Helen and Peringee Bore Granites. Age: 1800Ma.||||||07-FEB-11
31955|Chararoo Supersuite|50425|5|Briefly described|p1.1, 1.3, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Province.  Age: ~1800Ma. Intrudes: Gascoyne Complex.||||||07-NOV-08
31473|Charlotte Sandstone|12758|4|Described|p21, p10 Fig.10|Early Cretaceous|Early Cretaceous|Of the Parmelia Group. Predominantly sandstone with a few thin shale beds. Unconformably overlain by Warnbro Group. Thickness in type section: 589m. Geological Province: Vlaming Sub-basin.||||||27-JUL-09
31473|Charlotte Sandstone|14227|5|Briefly described|Enclos. 2|Valanginian|Valanginian|Of Parmelia Group. Overlies Hawley Member (Carnac Formation). Presented as Charlotte Sst.||||||07-FEB-11
31473|Charlotte Sandstone|24443|5|Briefly described|Fig.31|Early Cretaceous|Late Jurassic|Of Parmelia Group. Conformably overlies Carnac Formation. Overlain by Warnbro Group (unconformable) and Bunbury Basalt. Geological Province: Perth Basin.||||||27-JUL-09
31473|Charlotte Sandstone|50108|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Parmelia Group. Geological Province: Perth Basin.||||||27-JUL-09
31473|Charlotte Sandstone|60376|5|Briefly described|p17 Fig. 4.|Early Cretaceous|Early Cretaceous|Geological Province: Perth Basin. Of the Parmelia Group. Overlain unconformably by Gage Sandstone (Warnbro Group). Underlain by Carnac Formation (Permelia Group).||||||07-FEB-11
31473|Charlotte Sandstone|69182|6|Mentioned|Ch2 p15|Lower Cretaceous|Lower Cretaceous|Perth Basin. ||Parmelia Group||||
31473|Charlotte Sandstone|69297|6|Mentioned|p175, p189|Berriasian|Tithonian|Vlaming Sub-basin, South Perth Basin. ||Parmelia Group||||
31473|Charlotte Sandstone|70097|5|Briefly described|p19 Fig.3|Berriasian|Berriasian|Southern Perth Basin. Vlaming Sub-basin, Bunbury Trough.||Parmelia Group||Overlies Carnac Formation. Is overlain by Bunbury Basalt (Warnbro Group).|Sandstone.|30-SEP-16
31473|Charlotte Sandstone|70099|6|Mentioned|Fig.4|Berriasian|Berriasian|||Parmelia Group.||||
31473|Charlotte Sandstone|71377|5|Briefly described|p7|Early Cretaceous|Early Cretaceous|Perth Basin.||Parmelia Group||||
31473|Charlotte Sandstone|71958|4|Described|p2, p9-p10, p15, p34, p36-p37|Berriasian|Berriasian|Vlaming Sub-basin, Perth Basin. Briefly described by Backhouse (1984) before being formalised as a unit by Crostella and Backhouse (2000). A syn-rift reservoir unit lying below the Gage Sandstone. Estimated storage capacity is: 505.6 million tonnes at P90, 1983 million tonnes at P50 and 5453 million tonnes at P10. Intersected in six wells. subcrops over a vast area at the "Valanginian unconformity." Deposited in fluvial to deltaic environments. Good potential for CO2 storage. See also p41, p49, p51, p83-p84, p98, p117-p118, p140, p149, p163.||Parmelia Group||Unconformably overlain by the Gage Sandstone (Warnbro Group). Overlies the Carnac Formation.|Massive sandstones.|
80796|Charlotte Supersequence|71958|2|Defined|p40-p41, p45-p46|Valanginian|Late Berriasian|Vlaming Sub-basin. The name is derived from the Charlotte Sandstone with which it largely coincides. The type locality is defined in Charlotte 1 (-31.80879499, 115.45037501) between 1574.4 and 2163.4 m (total thickness of 589m). Sequence stratigraphy. Fluvial to deltaic succession on the basis of palynology. Penetrated in six wells in the basin. Deposited over approximately 1.3 million years. Features the diagnostic fossils F. tumida, B. eneabbaensis, P. charlottensis, P. punctate, T. baculata, ?Moorodinium sp. (Helby et al, 1987 and Partridge 2006). This unit has a similar thickness and extent to the Charlotte sandstone. This supersequence is present in Bouvard 1, Charlotte 1, Minder Reef 1, Mullaloo 1, Parmelia 1 and Peel 1 and exhibits westward thickening growth wedge geometry in the Bathurst syncline. The base of this unit is equivalent to the major sequence boundary "126" (Haq et al., 1987), the top of E. torynum of Helby et al (1987) and near top "TS K1" sequence of Seggie (1990). See also p48-p50, p80-p83, p87, p91, p101.||||Unconformably overlain by the South Perth Supersequence (Warnbro Megasequence). Unconformably overlies the Hawley Member of the Carnac Formation.|Very fine to very couarse quartzose sandstone with minor interbedded mudstone and coal.|
34925|Chatarie Well Granite|22902|5|Briefly described|68|||Geol province Southern Cross Province||||||
34925|Chatarie Well Granite|24167|5|Briefly described|p26, p7 Fig.3, p31 Fig 20|||Intrudes Butcher Bird Granite.  Geological Province: Yilgarn Craton||||||
34925|Chatarie Well Granite|24335|5|Briefly described|Map legend|Archean|Archean|Age: c.2711Ma.  Geological Province: Yilgarn Craton||||||07-NOV-08
34925|Chatarie Well Granite|70156|4|Described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma).|2698+\-4 Ma (isotopic)||||Coarse-grained monzogranite; metamorphosed|
34925|Chatarie Well Granite|70794|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton. Also 2_5m_interpgeop15_lut.csv.|2698+/-4 Ma||||Coarse grained monzogranite; metamorphosed.|
34925|Chatarie Well Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
34925|Chatarie Well Granite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||2698+/-4 Ma.||||Coarse-grained monzogranite; metamorphosed.|
33200|Cheearra Monzogranite|24533|5|Briefly described|p5, 7|Archean|Archean|A major component of the Yule Granitoid Complex. Leucocratic biotite (-hornblende) tonalite or granodiorite, with subordinate monzogranite. Age: c. 3065Ma.||||||07-NOV-08
33200|Cheearra Monzogranite|24554|5|Briefly described|p8|||Of the Yule Granitoid Complex. Geological Province: East Pilbara Granite-Greenstone Terrane.||||||
33200|Cheearra Monzogranite|50146|5|Briefly described|Map Legend|Archean|Archean|Of the Yule Granitoid Complex. Geological Province: Pilbara Craton.||||||07-NOV-08
33200|Cheearra Monzogranite|50370|5|Briefly described|Map Legend|Archean|Archean|Of Yule Granitoid Complex. Geological Province: Pilbara Craton||||||07-NOV-08
33200|Cheearra Monzogranite|50379|5|Briefly described|Map Legend|Archean|Archean|Of Yule Granitoid Complex. Geological Province: Pilbara Craton.||||||07-NOV-08
33200|Cheearra Monzogranite|63372|4|Described|Map Legend|Archean|Archean|Of the Yule Granitoid Complex. Geological Province: East Pilbara Granite-Greenstone Terrane.  Age: 2937-2933Ma. Monzogranite to granodiorite; massive to strongly foliated and gneissic; metamorphosed.||||||07-NOV-08
33200|Cheearra Monzogranite|63441|5|Briefly described|p10 Tb. 2|Archean|Archean|Of Sisters Supersuite. Ages: 2937+/-7Ma and 2933+/-4Ma. Geological province: Pilbara Craton.||||||07-FEB-11
33200|Cheearra Monzogranite|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Unit in Sisters Supersuite. 2952-2933 Ma. Metamonzogranite; weakly to strongly foliated; locally well developed banding; includes pegmatite and granite dykes.||||||
33200|Cheearra Monzogranite|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|c. 2952 Ma|Of the Sisters Supersuite.|||Metamonzogranite; weakly to strongly foliated; locally well developed banding; includes pegmatite and granite dykes.|30-APR-14
33200|Cheearra Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Sisters Supersuite|||Metamonzogranite; weakly to strongly foliated; locally well-developed banding; includes pegmatite and granite dykes. Metamonzogranite to metagranodiorite gneiss.|
33200|Cheearra Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; North Pilbara Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|2952 Ma (isotopic)|Unit of Sisters Supersuite.|||Metamonzogranite; weakly to strongly foliated; locally well-developed banding; includes pegmatite and granite dykes; metagranodioritic gneiss.|
33200|Cheearra Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, granodiorite|
33200|Cheearra Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||Max age 2937+/-7 Ma, Min 2933+/-4 Ma|Sisters Supersuite|||Metamonzogranite; weakly to strongly foliated; locally well-developed banding; includes pegmatite and granite dykes.|
39510|Chessman Granodiorite|63417|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite.  Age: 3318-3314Ma. Geological Province: Pilbara Craton. Metamorphosed biotite granodiorite and tonailte; medium- to coarse-grained; strongly foliated to gneissic.||||||07-NOV-08
39510|Chessman Granodiorite|63441|5|Briefly described|p8 Tb. 2|Archean|Archean|Of Emu Pool Supersuite. Ages: 3318+/-4Ma and 3314+/-6Ma. Geological province: Pilbara Craton.||||||07-FEB-11
39510|Chessman Granodiorite|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.|c.3314 Ma (Wyatt et al. 2001).|Of Mount Edgar Granitoid Complex.|||Biotite granodiorite and tonalite; medium- to coarse-grained; strongly foliated to gneissic.|
39510|Chessman Granodiorite|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|3318 - 3314 Ma.|Of Emu Pool Supersuite.|||Metamorphosed biotite granodiorite and tonalite; medium- to coarse-grained; strongly foliated to gneissic.|
39510|Chessman Granodiorite|65827|2|Defined|p6 Tb.2, p9 Fig 3, p13 Tb.4, p23, p58|Paleoarchean|Paleoarchean|New name. A narrow, 18 x 3 km intrusion named after Chessman Well. 3318+/4 Ma (SHRIMP U-Pb zircon; Nelson 2005) to 3314+/-6 Ma (Nelson 2005). Intruded by  metamorphosed mafic-ultramafic rocks correlated with Warrawoona Group.||Of Emu Pool Supersuite.||Intruded by Kennell Granodiorite, intrudes Fig Tree Gneiss, Underwood Gneiss, Duffer Formation, Apex Basalt.|Gneissic to strongly foliated granodiorite and tonalite.|21-MAY-14
39510|Chessman Granodiorite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Age derived from sample of medium grained, strongly foliated to gneissic leucocratic biotite granodiorite (169040.1.pdf) and is the age of crystallisation for granodiorite protolith.|3314 +/- 6 Ma (SHRIMP)||||Meta biotite granodiorite and metatonalite; medium to coarse grained; strongly foliated to gneissic.|
39510|Chessman Granodiorite|69566|6|Mentioned|p236|||Mount Edgar Granitoid Complex, East Pilbara Granite-Greenstone Terrane.||Emu Pool Supersuite.||||
39510|Chessman Granodiorite|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA 169040 (biotite granodiorite) yielded an interpreted igneous crystallisation age of 3314+\-6 Ma for the granodiorite (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3318-3314 Ma (isotopic)|Unit of Emu Pool Supersuite.|||Metamorphosed biotite granodiorite and metatonalite; medium to coarse grained; strongly foliated to gneissic|
39510|Chessman Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite, monzogranite|
39510|Chessman Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||Max age 3318+/-4 Ma, min 3314+/-6 Ma.|Emu Pool Supersuite|||Metamorphosed biotite granodiorite and metatonalite; medium to coarse grained; strongly foliated to gneissic.|
36846|Chester Formation|23727|4|Described|p7|||Geological Province: Carlingup Terrane. Max. thickness: >750 m.||||||
36846|Chester Formation|23728|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Bandalup Ultramafics. Geological Province: Yilgarn Craton.||||||07-NOV-08
36846|Chester Formation|23752|4|Described|p2|Archean|Archean|Geological Province: Carlingup Terrane.||||||07-NOV-08
36846|Chester Formation|23754|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Bandulup Ultramafics. Geological Province: Yilgarn Craton.||||||07-NOV-08
36846|Chester Formation|24165|6|Mentioned|p43|Archean|Archean|Carlingup Terrane, Ravensthorpe greenstone belt.||||||
36846|Chester Formation|64580|4|Described|map legend|Archean|Archean|Pelite with minor psammite and psephite; minor felsic volcanics and volcaniclastics; banded iron-formation.||||||15-DEC-08
36846|Chester Formation|65487|5|Briefly described|p6|||Lowermost unit in the Carlingup Greenstone Belt; consists of pelitic and psammitic rocks interbedded with metachert and metamorphosed BIF, and minor metapsephite and metamorphosed felsic volcanic and volcaniclastic rocks. At least 750 m thick.||||||10-FEB-14
36846|Chester Formation|68108|5|Briefly described|p651 Tb.4|Mesoarchean|Mesoarchean|Southern Cross Domain. Age of rhyolite; stratigraphic relationship uncertain. U-Pb geochronology by Nelson (1995).|2958 +/- 4 Ma||||Rhyolite.|08-OCT-14
36846|Chester Formation|69404|5|Briefly described|p10, p10 Fig.11|||Carlingup Terrane.||||Faulted against the overlying Bandalup Ultramafics.|Shales, siltstones, lithic sandstones, banded iron formation and minor chert, felsic to intermediate volcanic rocks.|
36846|Chester Formation|69559|5|Briefly described|500k_geologyp08_lut.csv|Archean|Archean||||||Pelite with minor psammite and psephite; minor felsic volcanics and volcaniclastics; banded iron formation.|
36846|Chester Formation|69617|5|Briefly described|p155|||Ravensthorpe greenstone belt, Southern Cross Domain, Yilgarn Craton. Parts of the stratigraphy may be equivalent to Honman Formation.|||||Felsic volcanic rocks, sedimentary rocks and komatiites.|
36846|Chester Formation|70156|4|Described|500k_interpgeop14_lut.csv|Mesoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma).|3200-2958 Ma (inferred)||||Pelite with minor psammite and psephite; minor felsic volcanics and volcaniclastics; banded iron-formation|
36846|Chester Formation|70794|4|Described|500k_interpgeop14_lut.csv|Mesoarchean|Mesoarchean|Youanmi Terrane, Yilgarn Craton. Also 2_5m_interpgeop15_lut.csv, where age range given as 3131-2958 Ma inferred.|3200-2958 Ma inferred.||||Pelite with minor psammite and psephite; minor felsic volcanics and volcaniclastics; banded iron formation.|
36846|Chester Formation|70802|5|Briefly described|500k_interpgeop14_lut.csv|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Youanmi Terrane events.|3200-2958 Ma (inferred)||||Pelite with minor psammite and psephite; minor felsic volcanics and volcaniclastics; banded iron-formation|
36846|Chester Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Youanmi Terrane.|||||Pelite with minor psammite and psephite; minor metamorphosed felsic volcanic and volcaniclastic rocks, and banded iron-formation.|
36846|Chester Formation|72491|6|Mentioned|p46|||Witt (1998). NE Ravensthorpe Belt, Southern Cross Terrane, Yilgarn Craton. Metamorphic effects described.||||||
23483|Cheyne Springs Formation|22905|4|Described|p52 Fig. 2, p53-54|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group. Overlain by the Kiangi Creek Formation. Conformably overlies the Blue Billy Formation.  Max. thickness: 300m.||||||24-JAN-06
23483|Cheyne Springs Formation|23403|4|Described|p7|Mesoproterozoic|Mesoproterozoic|Of Irregully Formation.||||||24-NOV-09
23483|Cheyne Springs Formation|24115|4|Described|p4 Fig.2|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group. Maximum Thickness: 300m. Overlies the Blue Billy Formation. Overlain by the Kiangi Creek Formation. Geological Province: Edmund Basin.||||||
23483|Cheyne Springs Formation|24183|2|Defined|p4 Fig.3, p11, p12|Calymmian|Statherian|Of the Edmund Group (Martin et al. 1999a). Max. Thickness: 300m. Overlies the Blue Billy Formation. Disconformably overlain by the Kiangi Creek Formation. Age: 1620-1462 Ma.||||||21-MAR-11
23483|Cheyne Springs Formation|24544|4|Described|p44 Fig.32|Mesoproterozoic|Mesoproterozoic|Of Edmund Group. Overlies Blue Billy Formation. Overlain by Kiangi Creek Formation.||||||24-FEB-05
23483|Cheyne Springs Formation|42013|5|Briefly described|Map legend|Proterozoic||||||||
23483|Cheyne Springs Formation|42471|4|Described|p20|||||||||
23483|Cheyne Springs Formation|42472|5|Briefly described|Map legend|||||||||
23483|Cheyne Springs Formation|44142|4|Described|p313 Tb.4-4, p317-318, p326 Tb.4-5|||Previously mapped with Irregully Formation, Top Camp Formation or Kiangi Creek Formation. Separated from the former by Chuck (1984). 200-700m thick, shallow-water shelf, shelf edge and slope deposits. Contains stromatolites and oncolites. Within Florry Subgroup of Chuck (1984).||Edmund Subgroup.||Conformably overlies Gooragoora Sandstone where present. Is overlain by Irregully Formation. Correlated with basal Uaroo Group.|Dolomite, dololutite, dolomitic breccia; minor mudstone, sandstone, siltstone.|
23483|Cheyne Springs Formation|50225|4|Described|p387 Fig. 2, p394|||Of Edmund Group. Undulatory laminated dolomudstone interbedded with siltstone, dolomitic siltstone. Conformably overlies Blue Billy Fm; unconformably overlain by Kiangi Creek Fm.  Max. thickness: 300m. See also p389.||||||07-FEB-11
23483|Cheyne Springs Formation|50292|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Geological Province: Edmund Basin.  Of the Edmund Group (Bangemall Supergroup). Overlies: Blue Billy Formation.  Underlies: Kiangi Creek Formation.||||||07-NOV-08
23483|Cheyne Springs Formation|50312|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Edmund Group. Geological Province: Edmund Basin. Dololutite, dolarenite, dolrudite, mudstone, siltstone, and minor sandstone.||||||31-MAY-04
23483|Cheyne Springs Formation|50313|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin. Underlies: Kiangi Creek Formation. Overlies: Blue Billy Formation.||||||07-NOV-08
23483|Cheyne Springs Formation|50380|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin.||||||07-NOV-08
23483|Cheyne Springs Formation|60301|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin. Dololutite, dolarenite, dolorudite, mudstone, siltstone, and minor sandstone.||||||07-NOV-08
23483|Cheyne Springs Formation|63866|5|Briefly described|p162|||||Edmund Group||||
23483|Cheyne Springs Formation|63869|4|Described|p28, p31, p32, p42, Plate 1|Calymmian|Statherian|Defined by Chuck (1984); revised after abandonment of Jillawarra Formation and redefinition of Kiangi Creek Formation (Martin and Thorne, 2002): basal 700 m of argillaceous rocks in Cheyne Springs Formation type section now assigned to Blue Billy Formation. 50-300 m thick, usually <200 m.|c.1620-1465 Ma.|Unit in Edmund Group.||Gradationally overlies Blue Billy Formation. Is disconformably overlain by Kiangi Creek Formation.|Interbedded dololutite, dolomitic siltstone and siltstone; thin beds of dolomitic sandstone and quartz sandstone; rare conglomerate.|
23483|Cheyne Springs Formation|64580|4|Described|map legend||Mesoproterozoic|Of Edmund Group. Siltstone and mudstone; sandstone, and dolostone; locally sulfidic.||||||
23483|Cheyne Springs Formation|64728|5|Briefly described|p95 Fig.2, p96. |Mesoproterozoic|Mesoproterozoic|Deeper marine siliciclastic and carbonate facies.||Unit in Edmund Group.||Overlies Blue Billy Formation. Is unconformably overlain by Kiangi Creek Formation.||
23483|Cheyne Springs Formation|65830|4|Described|p4, p5, p6, p9-10, p14; Plates 1,2|Calymmian|Statherian|50m to 300m thick. Interpreted as an association of shelf and pelagic dolostones that record a slight shallowing of the Edmund Basin.||Of the Edmund Group||Gradationally overlies Blue Billy Formation. Disconformably overlain by the Kiangi Creek Formation.|Comprises interbedded dololutite, dolomitic siltstone, and siltstone, together with minor fine- to medium-grained dolomitic sandstone and quartz sandstone.|
23483|Cheyne Springs Formation|66241|6|Mentioned|pp1-4. |||||Unit in Edmund Group.||Overlies Blue Billy Formation. Is overlain disconformably by Kiangi Creek Formation.||
23483|Cheyne Springs Formation|67374|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Edmund Basin.||Unit in Edmund Group.|||Dololutite, dolarenite, dolorudite, mudstone, siltstone and minor sandstone.|
23483|Cheyne Springs Formation|68285|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin.||Of the Edmund Group.||Underlain by Blue Billy Formation. Overlain by Kiangi Creek Formation.|Dololutite, dolarenite, dolorudite, mudstone, siltstone, and minor sandstone.|
23483|Cheyne Springs Formation|68286|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin.||Of the Edmund Group||Underlain by the Blue Billy Formation. Overlain by the Kiangi Creek Formation.|Dololutite, dolarenite, dolorudite, mudstone, siltstone, and minor sandstone.|
23483|Cheyne Springs Formation|69003|5|Briefly described|p34|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||Edmund Group.||Overlies Blue Billy Formation. Is overlain unconformably by Kiangi Creek Formation.||
23483|Cheyne Springs Formation|69024|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Of the Edmund Group.||Underlain by the Blue Billy Formation.|Dololutite, dolarenite, dolorudite, mudstone, siltstone and minor sandstone.|05-MAY-14
23483|Cheyne Springs Formation|69027|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Of the Edmund Group.||Underlain by the Blue Billy Formation. Overlain by the Kiangi Creek Formation.|Dololutite, dolarenite, dolorudite, mudstone, siltstone, and minor sandstone.|05-MAY-14
23483|Cheyne Springs Formation|69028|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin. Mapped with Blue Billy and Gooragoora Formations as one unit.||Of the Edmund Group.|||Siltstone and mudstone, sandstone and dolostone; locally sulfidic.|06-MAY-14
23483|Cheyne Springs Formation|69166|4|Described|geologyp_lut.csv|Mesoproterozoic|Paleoproterozoic|||Edmund Group||Conformably overlies Blue Billy Formation,|Undivided; dololutite, dolarenite, dolorudite, mudstone, and thin to thickly bedded sandstone and siltstone; minor dolostone.|
23483|Cheyne Springs Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|||Part of Edmund Group, Depositiional package 2.||Unit of Edmund Group.||||
23483|Cheyne Springs Formation|69596|6|Mentioned|p12 Fig.7|||Edmund Basin.||Edmund Group.||||
23483|Cheyne Springs Formation|70019|5|Briefly described|p93-94|Mesoproterozoic|Mesoproterozoic|Geological province: Gascoyne Province, Capricorn Orogen.||Unit of Edmund Group.||Overlain by Kiangi Creek Formation. Underlain by Blue Billy Formation.||
23483|Cheyne Springs Formation|70795|4|Described|100k_geologyp_lut.csv|Mesoproterozoic|Paleoproterozoic|Also 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 148973.1.pdf West Australian Craton, Edmund Basin|1679-1517 Ma|Edmund Group||Conformably overlies Blue Billy Formation, Disconformably overlain by Kiangi Creek Formation|Dololutite, dolarenite, dolorudite, mudstone, thin to thick bedded sandstone and siltstone; minor dolostone.|
23483|Cheyne Springs Formation|70814|4|Described|p3, p5, p8-p10, p20, p22, p24|||Edmund Basin. Together with the Gooragoora and Blue Billy Formations forms Depositional Package 2 of the Edmund Group. Ranges in thickness from 50-300m but only locally exceeds 200m. Interpreted as a shelf and pelagic deposit. Age poorly constrained.||Edmund Group||Conformably overlies the Blue Billy Formation. Overlain by the Kiangi Creek Formation.|Dololutite, dolarenite, dolorudite, mudstone, siltstone and minor sandstone.|
23483|Cheyne Springs Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||dololutite, dolostone/dolomite breccia, dolarenite, crystalline dolostone/dolomite, siltstone, mudstone|
23483|Cheyne Springs Formation|72705|5|Briefly described|p3-4|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||Edmund Group.||Overlies Blue Billy Formation. Is overlain unconformably by Kiangi Creek Formation.|Siliciclastic and carbonate sedimentary rocks.|
33196|Chiall Formation|23529|4|Described|p16|Paleoproterozoic|Paleoproterozoic|Of the Miningarra Subgroup.  Thickness: ~2000m.  Geological Province: Earaheedy Basin.||||||17-MAR-09
33196|Chiall Formation|23530|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Miningarra Subgroup, Earaheedy Basin||||||07-NOV-08
33196|Chiall Formation|23561|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Earaheedy Group, Earaheedy Basin.||||||07-NOV-08
33196|Chiall Formation|23581|5|Briefly described|Map legend||Paleoproterozoic|Of the Earaheedy Group in the Earaheedy Basin||||||07-NOV-08
33196|Chiall Formation|23589|4|Described|p28|||Incorporates the sandy upper of the Wandiwarra Formation. Of Earaheedy Group. Overlain by Wandiwarra Member; underlain by Windidda Formation. Earaheedy Basin. Max. thickness 500 m.||||||17-MAR-09
33196|Chiall Formation|23611|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|Age: 1850 Ma (SHRIMP U-Pb). See also page 33 Appendix 1. Of Miningarra Subgroup. Geological Province: Earaheedy Basin.||||||07-NOV-08
33196|Chiall Formation|23890|5|Briefly described|p21 Fig.11|||Of Miningarra Subgroup. Geological Province: Earaheedy Basin.||||||
33196|Chiall Formation|24017|4|Described|p16|Paleoproterozoic|Paleoproterozoic|Of the Miningarra Subgroup. Geological Province: Earaheedy Basin.||||||07-NOV-08
33196|Chiall Formation|24018|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Earaheedy Group.  Geological Province: Earaheedy Basin.||||||07-NOV-08
33196|Chiall Formation|24578|4|Described|p776 Fig.1, p778 Fig.3|Paleoproterozoic|Paleoproterozoic|Of the Miningarra Subgroup (Earaheedy Group). Overlies the Windidda Formation. Age: ~1800 Ma. Geological Province: Earaheedy Basin||||||07-NOV-08
33196|Chiall Formation|50188|2|Defined|p2 Fig. 1, p3, p6|Paleoproterozoic|Paleoproterozoic|Of Miningarra Subgroup (Earaheedy Gp). Supersedes 'Wandiwarra Formation' and 'Princess Ranges Quartzite'. Contains Karri Karri, Wandiwarra and Princess Ranges Members. Max. thickness:1500m. Conformably overlies Frere Formation. Geol.Prov: Earaheedy Basin.||||||07-NOV-08
33196|Chiall Formation|50195|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Miningarra Subgroup (Earaheedy Group).  Includes the Princess Ranges, Wandiwarra and Karri Karri Members.  Geological Province: Earaheedy Basin.||||||07-NOV-08
33196|Chiall Formation|50222|4|Described|p320 Fig. 3, p329|Paleoproterozoic|Paleoproterozoic|Of the Miningarra Subgroup (Earaheedy Group).  Includes the Karri Karri, Princess Ranges and Wandiwarra Members.  Age: c.2.0Ga (Hallovic et al, 2004).  Max. thickness: ~1000m.  Geol. Prov: Earaheedy Basin.  See also p319 Fig. 2.||||||07-NOV-08
33196|Chiall Formation|50223|5|Briefly described|p345 Fig. 2, p346|Paleoproterozoic|Paleoproterozoic|Of the Miningarra Subgroup (Earaheedy Group).  Includes Karri Karri, Wandiwarri and Princess Ranges members.  Geological Province: Earaheedy Basin.||||||07-NOV-08
33196|Chiall Formation|50224|5|Briefly described|p368 Tb.1|Paleoproterozoic|Paleoproterozoic|Of the Minningarra Subgroup (Earaheedy Group).  Sandstone; kaolinitic siltstone, silty sandstone. Contains the Princess Ranges, Wandiwarra and Karri Karri members. Max. thickness: ~1000m. Geological Province: Earaheedy Basin.||||||07-FEB-11
33196|Chiall Formation|50226|5|Briefly described|p423, p424 Fig. 5|||Basal unit of Miningarra Subgroup (Earaheedy Group).  Coarse and mature clastic units, commonly glauconitic.  Overlain by Wongawol Formation.  Geological Province: Earaheedy Basin.||||||09-DEC-04
33196|Chiall Formation|50309|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Earaheedy Basin.  Of the Miningarra Subgroup (Earaheedy Group).  Includes and overlies: Karri Karri Member.||||||07-NOV-08
33196|Chiall Formation|50319|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Miningarra Subgroup (Earaheedy Group). Geological Province: Earaheedy Basin. Sandstone, variable texture and composition, stratigraphic position uncertain.||||||07-NOV-08
33196|Chiall Formation|50334|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Miningarra Subgroup (Earaheedy Group). Geological Province: Earaheedy Basin||||||07-NOV-08
33196|Chiall Formation|50378|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Miningarra Subgroup (Earaheedy Group). Overlies Windidda Formation. Geological Province: Earaheedy Basin.||||||07-NOV-08
33196|Chiall Formation|50626|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Earaheedy Group.  Sandstone siltstone and shale.  Geological Province: Earaheedy Basin.||||||07-NOV-08
33196|Chiall Formation|63866|5|Briefly described|p166|||Eraheedy Basin.||Miningarra Subgroup||Overlain by the Wongawol Formation.||
33196|Chiall Formation|64161|6|Mentioned|p592|Calymmian|Statherian|Glauconite K-Ar age of 1710-1670 Ma and Rb-Sr glauconite age of 1674-1556 Ma by Preiss et al. (1975).||Of Earaheedy Group.||||21-MAR-12
33196|Chiall Formation|64284|4|Described|p58 Fig. 1, p59|Paleoproterozoic|Paleoproterozoic|Of the Minningarra Subgroup (Earaheedy Gp). Combines as members, the former "Wandiwarra Formation" and "Princess Ranges Quartzite". Geol.prov: Earaheedy Basin. Shale, siltstone, mudstone intercalated with thick sst beds and intraclastic breccia.||||||07-FEB-11
33196|Chiall Formation|64285|5|Briefly described|p65, p66-67 Figs.1,2|Paleoproterozoic|Paleoproterozoic|Of Minningarra Subgroup (Earaheedy Group). Geological Province: Earaheedy Basin. Quartz sandstone, siltstone and mudstone.||||||07-FEB-11
33196|Chiall Formation|64580|4|Described|map legend||Paleoproterozoic|Of Miningarra Subgroup. Sandstone and siltstone; minor conglomerate.||||||15-DEC-08
33196|Chiall Formation|64725|6|Mentioned|p59.|||||Basal unit in Miningarra Subgroup.||Is overlain by Wongawol Formation.||03-APR-12
33196|Chiall Formation|64772|4|Described|p12, Plate 1, p10 Fig. 5|Paleoproterozoic|Paleoproterozoic|Comprises Karri Karri, Wandiwarra + Princess Ranges Members. Max.age:1875Ma. Affected by Shoemaker impact structure. Thick: 1000m. Geol.prov:central Earaheedy Basin. On Plate 1, Chiall Formation shown within Tooloo Subgroup [error?]. See also p8 Fig.4,  p17, p19 Fig.9, p20-21 Fig.10, p25 Fig.11, p26 Fig.13, p30, p31 Fig.18, p32, p33 Fig.21, p36, p39 Fig.25-26, p40 Fig.27, p43, p44 Fig.30, p45, p51, p70-71 App.4 Tb.4.2, p72-74 Fig.4.1, p75 App.4 Tb.4.3, p76-77 Fig.4.2, p78 App.4 Tb.4.4||Of Miningarra Subgroup (Earaheedy Group)||rests on Windidda Member; is overlain by Wongawol Formation|Comprises shale, siltstone + mudstone intercalated with thick sst beds+intraclastic breccia - more detail incl'd|25-NOV-13
33196|Chiall Formation|65264|5|Briefly described|p27, p32, p44 Appdx. 1|Paleoproterozoic|Paleoproterozoic|Of theMooloogool Subgroup ( Earaheedy Group). Includes Karri Karri and Wandiwarra Members. Age: 1850Ma (SHRIMP U-Pb, zircon). Geological province: Earaheedy Basin. Contains quartz-iron-oxide-manganese veins.||||||07-FEB-11
33196|Chiall Formation|65472|5|Briefly described|p1, p3 Fig.2|||Thickness: ~1000 m. Age: from Fig.2, after Pirajno et al. Earaheedy Basin.|2.0 Ma detrital zircon U-Pb SHRIMP youngest age|Of Miningarra Subgroup.|Includes Princess Ranges Member, Wandiwarra Member, Karri Karri Member.||silty and sandy mature clastic units, commonly glauconitic|24-SEP-15
33196|Chiall Formation|65692|4|Described|p1, p9-10, p18-25, p28-30, p34, p54-56|||See also p59-63, p65-66, p75-78, p80-81. Earaheedy Basin. c.1000m thick. U-Pb-Th and Hf data detailed.||Miningarra Subgroup.|Karri Karri, Princess Ranges, Wandiwarra Members.|Overlies Windidda Formation. Is overlain by Wongawol Formation.|Basal shale and siltstone layers intercalated with sandstone, grading upwards into coarse-grained sandstone and breccia sourced from the SW.|
33196|Chiall Formation|66427|5|Briefly described|p43-48, p51-55, p61-73           |||Replaces Wandiwarra Formation and Princess Ranges Quartzite and includes them as Members, along with basal Karri Karri Member; recognised as part of a single depositional episode. Age is of Wandiwarra Member. SHRIMP U-Pb detrital zircon age from Princess Ranges Member is 1876 +/- 19 Ma (Halilovic et al., 2004). c.1000 m thick.|1685 +/- 35 Ma (glauconite K-Ar; Horwitz, 1975).|Unit in Miningarra Subgroup.|Includes Karri Karri, Wandiwarra and Princess Ranges Members.|Overlies Frere Formation conformably; is overlain by Wongawol Formation.|Consists of shale, siltstone and mudstone intercalated with thick sandstone beds and intraclastic breccia.|
33196|Chiall Formation|68055|6|Mentioned|p77|Proterozoic|Proterozoic|Earaheedy Basin.||Miningarra Subgroup.||||
33196|Chiall Formation|69003|5|Briefly described|p13 Fig.17, p14|||Earaheedy Basin. c.1000m thick.||Miningarra Group.|Karri Karri, Wandiwarra, Princess Ranges Members.|Unconformably overlies Windidda Member (Frere Formation). Is overlain ?conformably by Wongawol Formation.||
33196|Chiall Formation|69152|5|Briefly described|GEOL_LUT_CSV files + geochron files|||||Miningarra Subgroup|Includes Karri Karri Member, Wandiwarra Member, Princess Ranges Member.|||
33196|Chiall Formation|69313|6|Mentioned|p22 Fig.4.2, p23, p25, p61, p101|Paleoproterozoic|Paleoproterozoic|||Minningarra Subgroup|Karri Karri, Princess Ranges, Wandiwarra Members.|Overlies the Windidda Member (Frere Formation). Overlain by the Wongawol Formation.|Sandstone.|08-SEP-17
33196|Chiall Formation|69596|5|Briefly described|p10-11|||Earaheedy Basin.||Miningarra Group.|Karri Karri, Wandiwarra, Princess Ranges Members.|||
33196|Chiall Formation|70153|4|Described|100k_geologyp10_lut.csv|Paleoproterozoic|Paleoproterozoic|500k_interpgeop14_lut.csv.|1876 +/- 19 Ma (isotopic) - 1600 Ma (inferred).|Miningarra Group|Includes Karri Karri Member, Wandiwarra Member||Sandstone and siltstone, minor conglomerate; glauconitic in lower part.|
33196|Chiall Formation|71042|6|Mentioned|p97||||||Includes the Karri Karri Member.|||
33196|Chiall Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone, shale|
33196|Chiall Formation|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen. Of Earaheedy Basin. Events: Edmundian Orogeny (1026 - 954 Ma); Mangaroon Orogeny (1682 - 1619 Ma); Stanley Fold Belt deformation (2005 - 1620 Ma); Mangaroon Orogeny D2m/M2m (1677 - 1659 Ma); Mangaroon Orogeny D1m/M1m (1682 - 1677 Ma). See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv.|1876+\-19 Ma; 1650 Ma|Unit of Miningarra Group.|Includes Karri Karri Member, Princess Ranges Member, Wandiwarra Member.||Sandstone and siltstone, minor conglomerate; glauconitic in lower part|
33196|Chiall Formation|71484|4|Described|p124-125,131-132|Orosirian|Orosirian|Geological province: Of Earaheedy Basin. Thickness: c. 1000m. Generally deepens in depositional facies across central part of the basin. Contains a distinct conglomerate breccia at the base of the unit interpreted to be a submarine hardground (Jones et al., 2001) and regarded as a significant hiatus. Matonia (2009) provided maximum age constraint of c. 1970 Ma; Halilovic et al. (2004) provided possible c. 1876 Ma age.||Unit of Miningarra Group.||Overlain by Wongawol Formation. Underlain unconformably by Frere Formation/Tooloo Group..|Fine-grained sandstone (quartz, minor chert, feldspar, glauconite and accessory tourmaline and zircon) and siltstone, interleaved with sandstone, conglomerate and breccia.|30-AUG-19
33196|Chiall Formation|71798|6|Mentioned|p110|||Earaheedy Basin.||||||
33196|Chiall Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin.|Max age 1876+/-19 Ma, Min ~1650 Ma.|Miningarra Group|||Sandstone and siltstone, minor conglomerate; glauconitic in lower part.|
35238|Chillerina Granodiorite|24166|4|Described|p15|Archean|Archean|Of the Pippingarra Granitoid Complex||||||07-NOV-08
35238|Chillerina Granodiorite|24327|5|Briefly described|Map Legend|Archean|Archean|Of the Pippingarra Granitoid Complex. Hornblende-biotite granodiorite to K-feldspar porphyritic monzogranite. Age: >2930Ma. Geological Province: Pilbara Craton||||||18-JUN-14
35238|Chillerina Granodiorite|24349|5|Briefly described|Map legend|Archean|Archean|Of the Pippingarra Granitoid Complex.  Age: c.2945-2930Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
35238|Chillerina Granodiorite|50302|5|Briefly described|Map Legend|Archean|Archean|Part of the Pippingarra Granitoid Complex. Age: c.2945Ma. Geological Province: Pilbara Craton.||||||18-JUN-14
35238|Chillerina Granodiorite|63420|5|Briefly described|Map legend|Archean|Archean|Of the Sisters Supersuite. Age: c.2945Ma. Geological Province: Pilbara Craton. Hornblende-biotite granodiorite; grades to K-feldspar porphyritic monzogranite; massive to moderately foliated; metamorphosed.||||||07-NOV-08
35238|Chillerina Granodiorite|63441|5|Briefly described|p10 Tb. 2|Archean|Archean|Of Sisters Supersuite. Ages: 2940+/-2Ma, 2945+/-2Ma and 2946+/-3Ma. Geological province: Pilbara Craton.||||||07-FEB-11
35238|Chillerina Granodiorite|68283|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|c.2945 Ma|Of the Sisters Supersuite.||Occurs as locally abundant inclusions within the Petermarer Monzogranite.|Hornblende-biotite granodiorite; grades to K-feldspar porphyritic monzogranite; massive to moderately foliated; metamorphosed.|
35238|Chillerina Granodiorite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Sisters Supersuite|||Granodiorite magmatically interleaved with porphyritic leucogranite. Granodiorite to K-feldspar porphyritic monzogranite; Metagranodiorite to metamonzogranite gneiss. Granodiorite and monzogranite net veined by diorite; weakly metamorphosed.|
35238|Chillerina Granodiorite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; North Pilbara Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|2946-2928 Ma (isotopic)|Unit of Sisters Supersuite.|||Granodiorite; magmatically interleaved with massive to weakly foliated, seriate to K-feldspar-porphyritic leucogranite, and monzogranite, strongly net-veined by diorite; weakly metamorphosed|
35238|Chillerina Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite, monzogranite|
35238|Chillerina Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||Max age 2946+/-3 Ma, min 2945+/-2 Ma.|Indee Suite|||Hornblende biotite granodiorite to K-feldspar porphyritic monzogranite; massive to moderately foliated; weakly metamorphosed.|
41375|Chimingadgi Trondhjemite|44229|5|Briefly described|Map legend|Archean|Archean|Part of the Mount Edgar Granitoid Complex.  Massive, even-grained, grey-white, biotite trondjhemite.||||||07-NOV-08
41375|Chimingadgi Trondhjemite|50189|4|Described|p15, 22|Archean|Archean|Pluton of Mount Edgar Granitoid Complex. Whitish-grey, massive, medium-grained trondhjemite. Intrudes the Euro Basalt and Munganbrina Monzogranite. Unconformably overlain by Fortescue Group.||||||07-NOV-08
41375|Chimingadgi Trondhjemite|50544|4|Described|p31, p21 Tb. 4|Archean|Archean|Of the Mount Edgar Granitoid Complex.  Intrudes Apex and Euro Basalts and the Mullugunya Granodiorite.  A whitish-grey, massive, non-foliated, medium-grained tronghjemite characterised by high plagioclase and quartz contents.||||||07-NOV-08
41375|Chimingadgi Trondhjemite|50555|5|Briefly described|Map legend|Archean|Archean|Of the Mount Edgar Granitoid Complex.  Massive, even-grained, grey-white biotite trondhjemite.  Geological Province: Pilbara Craton.||||||07-NOV-08
41375|Chimingadgi Trondhjemite|63417|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite.  Geological Province: Pilbara Craton. Biotite trondhjemite; medium-grained, massive, even grained; metamorphosed.||||||07-NOV-08
41375|Chimingadgi Trondhjemite|63441|5|Briefly described|p8 Tb. 2|Archean|Archean|Of Emu Pool Supersuite. Replaces Chimingadgi Suite. Geological province: Pilbara Craton.||||||07-FEB-11
41375|Chimingadgi Trondhjemite|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of Emu Pool Supersuite.|||Medium-grained, massive, biotite trondhjemite, seriate textured, weakly metamorphosed; hybrid amphibole-rich granitic rock with mafic and ultramafic xenoliths, metamorphosed.|
41375|Chimingadgi Trondhjemite|65827|5|Briefly described|p6 Tb.2, p9 Fig 3, p25|Paleoarchean|Paleoarchean|Williams (1999); originally part of Chimingadgi Suite (Collins 1983, 1993). Of Emu Pool Supersuite. Of Mount Edgar Granitic Complex. Intrudes Apex Basalt, Mullugunya Granodiorite. Foliated, medium-grained, partly seriate, whitish-grey biotite trondhjemite; some areas mafic xenolith-rich. Mis-spelt as Trondjhemite in Fig.3.||||||
41375|Chimingadgi Trondhjemite|69041|5|Briefly described|p8, p12-p13|||Pilbara Craton. Forms an elliptical pluton.||Chimingadgi Suite||Intrudes the Munganbrina Suite. Unconformably overlain by the Fortescue Group.|Medium-grained, biotite trondhjemite with a seriate texture and is moderately foliated.|
41375|Chimingadgi Trondhjemite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Emu Pool Supersuite|||Biotite trondhjemite; medium grained, massive, seriate textured; weakly metamorphosed. Hybrid amphibole rich granitic rock with mafic and ultramafic xenoliths; weakly metamorphosed.|
41375|Chimingadgi Trondhjemite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3325-3277 Ma (inferred)|Unit of Emu Pool Supersuite.|||Biotite trondhjemite; medium grained, massive, seriate textured; weakly metamorphosed; hybrid amphibole-rich granitic rock with mafic and ultramafic xenoliths; weakly metamorphosed.|
41375|Chimingadgi Trondhjemite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||trondhjemite|
41375|Chimingadgi Trondhjemite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|||Emu Pool Supersuite|||Biotite trondhjemite; medium grained, massive, seriate textured; weakly metamorphosed.|
38600|Chinaman Pool Chert Member|23783|5|Briefly described|p104|Archean|Archean|Of Towers Formation.||||||07-NOV-08
38600|Chinaman Pool Chert Member|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Geological Province: eastern Pilbara Craton.||||||07-NOV-08
38600|Chinaman Pool Chert Member|63441|5|Briefly described|p4 Tb. 1, p20|Archean|Archean|Redefined as part of Duffer Formation (Coongan Subgroup, Warrawoona Group, Pilbara Supergroup). Formerly of the Towers Formation. Geological province: Pilbara Craton.||||||07-FEB-11
38600|Chinaman Pool Chert Member|64621|5|Briefly described|Map legend|Archean|Archean|Of Duffer Formation (Coongan Subgroup, Warrawoona Group). White and grey layered chert; metamorphosed.||||||07-NOV-08
38600|Chinaman Pool Chert Member|66217|5|Briefly described|p17. |||||Unit in Duffer Formation.|||Layered sedimentary chert.|
38600|Chinaman Pool Chert Member|67130|6|Mentioned|p53|||||Duffer Formation|||Blue, white and red chert|
38600|Chinaman Pool Chert Member|68280|5|Briefly described|p27-28, p32|||||Duffer Formation|||Chert, intruded by dolerite sills.|13-JAN-23
38600|Chinaman Pool Chert Member|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Duffer Formation|||White and grey layered chert; metamorphosed|
38600|Chinaman Pool Chert Member|69590|4|Described|100k_geologyp_lut.csv|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event.|3463 Ma (inferred)|Unit of Duffer Formation.|||White and grey layered chert; metamorphosed|
23484|Chinty Formation|12471|6|Mentioned|p475 Fig.2. |Late Permian|Late Permian|||||||
23484|Chinty Formation|13615|3|Fully described|p4, p6-p8, p17, 18, p29-p30|Early Triassic|Late Permian|Peedamullah Shelf. Between 29-359m thick. Spores and Pollen zone provided. Intersected by numerous drillholes. The type section occurs in Onslow 1 between 2096 and 2258 m. Deposited in a moderate energy, shallow marine shelf to coastal environment. See also p41-p42, p47-p51, p58, p65p75-p76, p81, p83-p85, p87, p102-p103 App. 3, p119 App5,  Plates 2, 3.||Of Kennedy Group.||Conformably overlies the Abdul Sandstone. Unconformably overlain by the Flacourt Formation.|Silty grey sandstone with lesser siltstone, shale and limestone.|07-FEB-19
23484|Chinty Formation|23726|5|Briefly described|p8 Fig 2c|Late Permian|Late Permian|Overlying unit Locker Shale. Geological Province: Carnarvon Basin.||||||
23484|Chinty Formation|24044|5|Briefly described|p541||Permian|Geological Province: Carnarvon Basin||||||
23484|Chinty Formation|24331|5|Briefly described|p475 Fig.2|Permian|Permian|Unconformably overlies Byro Group. Unconformably overlain by Locker Shale. Marine to marginal marine. Geological Province: Barrow Sub-basin.||||||22-FEB-05
23484|Chinty Formation|40617|2|Defined|p5|Late Permian|Late Permian|||||||
23484|Chinty Formation|41271|3|Fully described|p105|||||||||
23484|Chinty Formation|41436|6|Mentioned|p41|||||||||
23484|Chinty Formation|41438|4|Described|p105|||||||||
23484|Chinty Formation|41440|4|Described|p134|||||||||
23484|Chinty Formation|41441|6|Mentioned|p152|||||||||
23484|Chinty Formation|41474|6|Mentioned|p63|||||||||
23484|Chinty Formation|41732|6|Mentioned|p534|||||||||
23484|Chinty Formation|42116|5|Briefly described|Fig.1 P6|||||||||
23484|Chinty Formation|43712|6|Mentioned|p10||Late Permian|||||||
23484|Chinty Formation|43722|6|Mentioned|p9||Late Permian|||||||
23484|Chinty Formation|43724|5|Briefly described|p28||Late Permian|||||||
23484|Chinty Formation|60384|6|Mentioned|p243 Fig 2b||Permian|Northern Carnarvon Basin.||||||
23484|Chinty Formation|60386|6|Mentioned|p297|Lopingian|Lopingian|Carnarvon Basin. Deltaic - nearshore - shelf. Age shown as Dorashamian.||||||
23484|Chinty Formation|64977|6|Mentioned|p493 Fig.3.|Permian|Permian|Thevenard Island area.||||||
23484|Chinty Formation|67200|5|Briefly described|p8 fig 6, |Permian|Permian|||||Overlain by Locker Shale|Sandstone, siltstone and limestone.|
23484|Chinty Formation|70066|5|Briefly described|Dampier: Fig.2. Exmouth: Fig.2|Wuchiapingian|Capitanian|See also Regional: Fig.6. Northern Carnarvon Basin.||||Is overlain by Locker Shale.||
23484|Chinty Formation|71146|5|Briefly described|p6|Guadalupian|Guadalupian|Southern Carnarvon Basin.|||||Sandstone.|
23484|Chinty Formation|71623|4|Described|p345, 346, 347, 348, 349, 351, p358|Capitanian|Wordian|Carnarvon Basin. Part of Cape Hay Clastic Cycle. Generally upward coarsening. Mostly non-marine. Contains Upper Stage 5 palynomorphs.||Of Kennedy Group.||Overlies Cody Formation unconformably.|Sandstone|
23484|Chinty Formation|72505|5|Briefly described|p890|Changhsingian|Wordian|Southern Carnarvon Basin. Correlates with the Dulhuntyispora granulata to Dulhuntyispora parvithola zones.||||Overlies the Binthalya Formation? Overlain by the Locker Shale.||18-MAR-20
23484|Chinty Formation|72910|4|Described|p1, p4, p7, p12-14, p18-20, p25.|Capitanian|Roadian|Restricted to Peedamullah Shelf, Carnarvon Basin. Type section in Onslow 1 (2096-2258 m). Age descibed as Kazanian to Tartarian.  Thickness <320m. See also p31, p33-35, p38, p41.||Kennedy Group||Underlies Locker Shale.|Silty grey sandstone with lesser siltstone, and shale.|
37147|Chocolate Hill Suite|23755|5|Briefly described|p75 Fig 37|Archean|Archean|||||||07-NOV-08
37147|Chocolate Hill Suite|23807|6|Mentioned|p137|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
37147|Chocolate Hill Suite|24590|5|Briefly described|p72|Archean|Archean|Of the Shaw Granitoid Complex. Age: 3338+/-52Ma.||||||07-FEB-11
26476|Choorun Formation|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Of Tarcunyah Group, Officer Basin.||||||
26476|Choorun Formation|23590|3|Fully described|p10|||Of Tarcunyah Group. Overlying unit Nooloo Formation. Underlying unit Rudall Complex. Geological Province: Officer Basin. Max. thickness >1800 m.||||||
26476|Choorun Formation|23602|6|Mentioned|p27 Fig. 9|||||||||
26476|Choorun Formation|23729|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Tarcunyah Group. Geological Province; Paterson Orogen.||||||
26476|Choorun Formation|23730|4|Described|p10|Neoproterozoic|Neoproterozoic|Age: 544+/-10 Ma (SHRIMP U-Pb zircon). Of Tarcunyah Group. O'lying unit Nooloo Formation. U'lying unit Rudall Complex. Geological Province: Officer Basin. Max. thickness: >1800 m.||||||
26476|Choorun Formation|23760|4|Described|p27|Proterozoic|Proterozoic|Of Tarcunyah Group. Geological Province: Officer Basin.||||||
26476|Choorun Formation|33849|4|Described|p124|||||||||
26476|Choorun Formation|36551|6|Mentioned|Table 22|||||||||
26476|Choorun Formation|37023|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26476|Choorun Formation|37212|3|Fully described|p12|||||||||
26476|Choorun Formation|37214|6|Mentioned|p6|||||||||
26476|Choorun Formation|37460|4|Described|Table3.VII|||||||||
26476|Choorun Formation|37707|6|Mentioned|Table I|||||||||
26476|Choorun Formation|41669|4|Described|p47|||See also Table 1||||||
26476|Choorun Formation|42278|6|Mentioned|p33|||||||||
26476|Choorun Formation|42352|6|Mentioned|p29|||Part of Yeneena Group||||||
26476|Choorun Formation|43055|4|Described|p28, Table 4|||Of Yeneena Group.||||||12-NOV-08
26476|Choorun Formation|43056|5|Briefly described|Map Legend|||Of Yeneena Group.||||||12-NOV-08
26476|Choorun Formation|43118|5|Briefly described|p22|||||||||
26476|Choorun Formation|43278|5|Briefly described|p644,Fig.2.||Neoproterozoic|of Yeneena Group.||||||
26476|Choorun Formation|43847|5|Briefly described|Map Legend||Proterozoic|||||||
26476|Choorun Formation|43867|5|Briefly described|Fig.2 p201|||Shown as part of informal Lower Yeneena Sub-Group.||||||
26476|Choorun Formation|44139|5|Briefly described|p277-280|Neoproterozoic|Neoproterozoic|Williams et al. (1976). 0-2000 m. Sandstone, siltstone, shale, conglomerate; minor dolomite. Western and central zones of Yeneena Basin. Conformably overlies Yandanunyah Formation; faulted against or unconformably overlain by the Savory Group; conformably overlies Broadhurst Formation. Overlain disconformably by Isdell Formation.| | ||||05-MAR-18
26476|Choorun Formation|50008|5|Briefly described|p46 Fig.3|||Of Tarcunyah Group. Geological Province: Officer Basin.||||||
26476|Choorun Formation|60470|5|Briefly described|p4 Fig. 2|Neoproterozoic|Neoproterozoic|in Officer Basin, of Tarcunyah Group. Sandstone; minor conglomerate, siltstone, and shale||||||
26476|Choorun Formation|62453|3|Fully described|p5 Fig. 3, 65|Cryogenian|Tonian|Of the Tarcunyah Group. Geological Province: Paterson Orogen. Unconformably overlies: Rudall Complex. Conformably overlain by Nooloo Formation. Conglomerate, sandstone. Thickness: ~1800m. ||||||
26476|Choorun Formation|64580|6|Mentioned|map legend|||Of Tarcunyah Group.||||||15-DEC-08
26476|Choorun Formation|64589|4|Described|dated_samples file||Neoproterozoic|U-Pb zircon maximum depositional age 574+/-62 Ma. Autolithic quartz-tourmaline mudstone, Curran Curran rockhole, of Tarcunyah Group, Officer Basin.||||||
26476|Choorun Formation|64777|5|Briefly described|p3 Fig.4 |Neoproterozoic|Neoproterozoic||||||Sandstone; minor conglomerate, siltstone and shale.|
26476|Choorun Formation|64943|5|Briefly described|p29|Neoproterozoic|Neoproterozoic|Of Tarcunyah Group. Paleocurrent data supports sediment transport from SW.||||||
26476|Choorun Formation|65403|6|Mentioned|p13.|||Facies equivalent of Gunanya Sandstone (?and Waters Formation).||Unit in Tarcunyah Group.||||
26476|Choorun Formation|65454|4|Described|p7 Fig.3, p10, p30 Fig.A1b|Cryogenian|Cryogenian|Of Tarcunyah Group. Upward-fining, fluviatile succession consisting of a coarse- to medium-grained sandstone, conglomerate, which appears to be folded in the Miles Orogeny. Unconformably overlies Rudall Complex; is overlain by Nooloo Formation.||||||
26476|Choorun Formation|65826|6|Mentioned|p7 Fig.4.|Neoproterozoic|Neoproterozoic|Officer Basin. Shown as in-part lateral equivalent of most of Tarcunyah Group, but unclear if intended to be include in the Group or not.||||||23-MAY-16
26476|Choorun Formation|67202|4|Described|p64-65, p231|Neoproterozoic|Neoproterozoic|Officer Basin. At least 1800m thick. Fluvial deposits.||Tarcunyah Group.||Unconformably overlies Rudall Complex. Is overlain by Nooloo Formation.|Cobble to pebble conglomerate, pebbly sandstone and coarse- to medium-grained sandstone.|
26476|Choorun Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|NW Paterson Orogen.||Tarcunyah Group.||||
26476|Choorun Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|Neoproterozoic|Neoproterozoic|||Unit of Tarcunyah Group.||||
26476|Choorun Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone, siltstone|
26476|Choorun Formation|71800|5|Briefly described|p26-p27|Early Cambrian|Ediacaran|Officer Basin.||||Overlies the McFadden Formation.|Tuffaceous rock.|
26476|Choorun Formation|72034|5|Briefly described|500k_interpgeop16_lut|Cryogenian|Tonian|Gibson Sub-basin, Officer Basin (Phase 1).||Tarcunyah Group|||Pebble to cobble conglomerate, pebbly sandstone, medium- to coarse-grained sandstone.|
24220|Christine Point Clay|36483|2|Defined|p69|Late Pleistocene|Late Pleistocene|Conformably on Mowanjum Sand; unconformable on Double Nob Fm. seawards. Overlain by Doctors Creek and Point Torment Fms. Max. thickness: 7.5m. Geological Province: Canning Basin. Slate grey, homogeneous to mottled clay........+ fossils.||||||07-AUG-07
24220|Christine Point Clay|37615|5|Briefly described|Table 1|||||||||
24220|Christine Point Clay|38013|6|Mentioned|Fig.3|||||||||
24220|Christine Point Clay|64449|5|Briefly described|p62 Tb. 2, p75-76|Quaternary|Quaternary|Defined by Semenuik (1980). Consists of grey kaolinitic clay with in situ mangrove stumps.||||||07-FEB-11
26478|Christopher Formation|42710|5|Briefly described|map legend|Proterozoic||Variation on Christopher Beds.||Of Oscar Range Group||||17-OCT-12
26478|Christopher Formation|42811|4|Described|p28|Neoproterozoic|Mesoproterozoic|of Oscar Range Group. ~2300 m thick.  Lithologically similar to Mount Wilson Sandstone.||||No contacts exposed, but are likely to be tectonic. Has variously been regarded as younger than Mt Wilson Sst, or possibly part of same unit. Intruded by dolerite sills.|Interbedded pebbleto boulder conglomerate, grey to white quartz sandstone, feldspathic sandstone, locally tuffaceous phyllitic sandstone, minor carbonate.|17-OCT-12
26478|Christopher Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Oscar Range Group.|||Interbedded boulder to cobble conglomerate, locally cross-bedded grey to white quartz and feldspathic sandstone, local tuffaceous phyllitic siltstone and minor carbonate, intruded by minor thin dolerite sills|
28454|Chuall beds|43631|6|Mentioned|p27|||||||||
28454|Chuall beds|45155|6|Mentioned|p42|||||||||
28454|Chuall beds|65074|4|Described|p351, p355 Tb.4-11, p358-360, p362|Devonian|Devonian|Of NW Birrindudu Basin. 140 m thick. Type area is SE of Sturt Creek Homestead. Non-fossiliferous.||||Probably overlies Redcliff Pound Group (unconformably). Probably equivalent to Pedestal beds.|Friable quartzose sandstone. Pellet-rich horizons and gritty bands.|
23486|Chulaar Group|41066|6|Mentioned|1 of 2 K05|||||||||
74835|Chunderloo Monzogranite|64891|5|Briefly described|p37 Fig. 2, p52-53 Tb. 1|Archean|Archean|Of the Jungar Suite. Age: 2665-2660Ma. Geological province: Murchison Domain. Monzogranite; metamorphosed.||||||07-FEB-11
74835|Chunderloo Monzogranite|65550|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Jungar Suite. Foliated metamonzogranite; locally schistose, may include amphibolite lenses; includes deeply weathered rock.||||||
74835|Chunderloo Monzogranite|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|2665 - 2640 Ma.|Unit in Jungar Suite.|||Biotite metamonzogranite, commonly with abundant K-feldspar phenocrysts/porphyroclasts; well-foliated to mylonitic; may include amphibolite lenses.|
74835|Chunderloo Monzogranite|67129|5|Briefly described|p19 Fig.20|Archean|Archean|Murchison Domain, Youanmi Terrane.||Jungar Suite.|||K-feldspar monzogranite.|
74835|Chunderloo Monzogranite|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. Jungar Suite not shown as 'Parent', but listed as 'Suite' for this unit.|||||Biotite metamonzogranite; commonly with abundant K-feldspar phenocrysts/porphyroclasts; well foliated to mylonitic; may include amphibolite lenses|
74835|Chunderloo Monzogranite|69583|5|Briefly described|p121; Plate 2|Archean|Archean||c.2660 ma.|Jungar Suite.|||Biotite metamonzogranite.|
74835|Chunderloo Monzogranite|69584|5|Briefly described|p5 Fig.2|Neoarchean|Neoarchean|||Jungar Suite|||Monzogranite.|
74835|Chunderloo Monzogranite|69586|5|Briefly described|p19, p22|Neoarchean|Neoarchean|Appears as Chunderloo Granite on p19.||Jungar Suite.||||
74835|Chunderloo Monzogranite|70139|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton.||Jungar Suite.|||Foliated biotite metamonzogranite.|
74835|Chunderloo Monzogranite|70796|5|Briefly described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton. See also 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, Tieraco100_2545_stratig.pdf.|ca 2665  2640 ma (inferred)|Jungar Suite|||Biotite metamonzogranite; commonly with abundant Kfeldspar phenocrysts/porphyroclasts; well foliated to mylonitic; may include amphibolite lenses.|
74835|Chunderloo Monzogranite|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv.|2665-2640 Ma|Unit of Jungar Suite.|||Biotite metamonzogranite; commonly with abundant K-feldspar phenocrysts/porphyroclasts; well foliated to mylonitic; may include amphibolite lenses|
74835|Chunderloo Monzogranite|71271|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton.|c.2655 Ma.|Jungar Suite.|||Biotite metamonzogranite, commonly with abundant K-feldspar phenocrysts/porphyroclasts, well-foliated to mylonitic, may include amphibolite lenses; (separately mapped) strongly foliated metagranitic rock, locally mylonitic or gneissic.|
74835|Chunderloo Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|||Jungar Suite|||Biotite metamonzogranite; commonly with abundant K-feldspar phenocrysts/porphyroclasts; well foliated to mylonitic; may include amphibolite lenses.|
74835|Chunderloo Monzogranite|72389|5|Briefly described|Map Legend|Archean|Archean|Yilgarn Craton. Gabanintha 1:100k map sheet 2644. Includes an unnamed foliated metagranitic member.|2655 Ma|Jungar Suite|||Biotite metamonzogranite; commonly with abundant K-feldspar phenocrysts/porphyroclasts; well foliated to mylonitic; may include amphibolite lenses.|28-AUG-20
74626|Church Hill Sand|64449|2|Defined|p75, p79 Tb. 5, p103|Holocene|Holocene|Overlies Barn Hill Formation and Mowanjum Sand.  Underlies Shoonta Hill Sand. Thick: 4m. Mainly structureless, but locally laminated to cross-laminated red quartz sand. See p103 for more information.||||||07-FEB-11
74626|Church Hill Sand|73213|5|Briefly described|958 Fig.3(a), 961 Fig.8|||Appears more often than not as Churchill Sand; see pages 955, 956-957 Figs.1-2, 959, 961-962, 966 Fig.14, 967-968, 970.||||Overlies Mowanjum Sand.||
31764|Churla Granite|23569|4|Described|p5 Tb. 1|Archean|Archean|Of the Narryer Terrane.   Coarse-grained, equigranular, leucocratic granulite-facies monzogranite||||||07-NOV-08
31764|Churla Granite|23574|5|Briefly described|Map Legend|Archean|Archean|Overlying Unit Yarra Yarra Granite. Underlying Unit Balla Granite.||||||07-NOV-08
31764|Churla Granite|23576|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Yarra Yarra Granite. Underlying unit Balla Granite.||||||07-NOV-08
31764|Churla Granite|23577|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Yarra Yarra Granite. Underlying unit Balla Granite.||||||07-NOV-08
31764|Churla Granite|24114|5|Briefly described|p5 Fig.4|Archean|Archean|Geological Province: Yilgarn Craton. Age: c. 2635 Ma.||||||07-NOV-08
31764|Churla Granite|43835|5|Briefly described|Map Legend|Archean|Archean|Age about 2635Ma.||||||07-NOV-08
31764|Churla Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, granite|
31764|Churla Granite|73526|6|Mentioned|p2 Fig.1, p3, p7-8|Neoarchean|Neoarchean|Western Narryer Terrane. See also Churla granite p4 Tb.1, age of 2636+/-7 Ma.|2635+/-5 Ma|||||
28297|Clanmeyer Siltstone|7433|6|Mentioned|p25 Fig.2. |||Canning Basin.||||||
28297|Clanmeyer Siltstone|22741|6|Mentioned|P24||Devonian|||||||
28297|Clanmeyer Siltstone|22767|5|Briefly described|Table3 P18, P20||Late Devonian|||||||
28297|Clanmeyer Siltstone|22776|4|Described|Table.3|Late Devonian|Late Devonian|Ammonoids and palynomorphs.||||||
28297|Clanmeyer Siltstone|24061|5|Briefly described|p180|||Geological Province: Canning Basin.||||||27-JAN-10
28297|Clanmeyer Siltstone|30110|6|Mentioned|p81|||See also P82. Frasnian age.||||||
28297|Clanmeyer Siltstone|32648|6|Mentioned|p32|||Famennian||||||
28297|Clanmeyer Siltstone|32865|6|Mentioned|p476|||See also P477. Famennian||||||
28297|Clanmeyer Siltstone|36224|5|Briefly described|Map legend|Late Devonian|Late Devonian|Siltstone, shale, minor limestone.||||||01-FEB-05
28297|Clanmeyer Siltstone|36634|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
28297|Clanmeyer Siltstone|36890|3|Fully described|p336|||||||||
28297|Clanmeyer Siltstone|38878|6|Mentioned|Map legend|Famennian|Famennian|||||||
28297|Clanmeyer Siltstone|41023|6|Mentioned|p292|||||||||
28297|Clanmeyer Siltstone|42030|5|Briefly described|p746|||||||||
28297|Clanmeyer Siltstone|42347|6|Mentioned|Fig.2 P1020|||||||||
28297|Clanmeyer Siltstone|42880|5|Briefly described|Fig.2,p1020|||||||||
28297|Clanmeyer Siltstone|43818|6|Mentioned|Fig.2.p39||Late Devonian|||||||
28297|Clanmeyer Siltstone|44143|4|Described|p.439 Table 4-19, p442|Devonian|Devonian|Up to 1500m thick; siltstone and shale; marine. Conformably overlies Babrongan Formation. Type section between 713 and 1736m in Babrongan 1 (MOUNT ANDERSON: 18 deg 23' 23" S; 123 deg 35' 37" E).||||||22-NOV-17
28297|Clanmeyer Siltstone|45041|6|Mentioned|Fig.45|||Middle Devonian||||||
28297|Clanmeyer Siltstone|45063|6|Mentioned|Fig. 9|||Devonian||||||
28297|Clanmeyer Siltstone|45153|2|Defined|App.3-38|late Famennian|late Famennian|See also App.3-36||||||
28297|Clanmeyer Siltstone|45158|3|Fully described|p26|||||||||
28297|Clanmeyer Siltstone|66127|6|Mentioned|p428.|||Subsurface unit. Contains a clymenid ammonoid of either the Rodeckiinae or Clymeniidae.||||||
28297|Clanmeyer Siltstone|69182|6|Mentioned|Ch4 p38, Ch4 p39, Ch4 p45|Carboniferous|Devonian|Canning Basin. Potential seal for the storage of carbon dioxde. See also Ch4 p64, Ch4 p87. ||||||
78345|Clapp Ridge Formation|68007|4|Described|p2,p4,p6-7,p10,p12,p14-15, Plates 1, 2|Givetian|Givetian|Of Allen (in prep.). Barbwire Terrace; Kidson Sub-basin. Shallow to marginal-marine sediments. The intervals between 1335 and 1626 m in Patience 1 well, and 1343 - 1630 m in Patience 2 well, are tentatively assigned to this unit. Characterised by a consistently high gamma response. Shaly facies may provide an effective seal over Tandalgoo Formation. Composite well log.||||Overlies Tandalgoo Formation unconformably. Is overlain unconformably by Reeves Formation or the Betty Formation (Grant Group).|Dominated by reddish-brown, argillaceous and dolomitic siltstone, with interbeds of silty dolomite and silty claystone.|24-FEB-20
78345|Clapp Ridge Formation|69182|6|Mentioned|Ch4 p9, Ch4 p13-p14|Middle Devonian|Middle Devonian|Canning Basin. See also Ch4 p42, Ch4 p45, Ch4 p47, Ch4 p50-p58, Ch4 p74, Ch4 p78, Ch4 p86.||||Overlies the Tandalgoo Formation. Overlain by the Mellinjerie Formation.||
78345|Clapp Ridge Formation|71146|5|Briefly described|p6|Eifelian|Emsian|Canning Basin.||||Overlies the Tandalgoo Formation. Overlain by the Mellinjerie Formation.|Mudstone.|
78345|Clapp Ridge Formation|71894|5|Briefly described|p4|Middle Devonian|Middle Devonian|Canning Basin.||||Overlies the Tandalgoo Formation. Overlain by the Mellinjerire Formation.|Shale.|
78345|Clapp Ridge Formation|72499|5|Briefly described|p7 Fig.6.|Middle Devonian|Middle Devonian|Located in the Willara Sub-basin and Broome Platform.||||Overlies Tandalgoo Formation. Underlies Mellinjerie Formation and shown as unconformably underlying Grant Group.|Includes shale.|
34585|Clark Well Monzogranite|22841|5|Briefly described|Map legend||Archean|||||||07-NOV-08
34585|Clark Well Monzogranite|22890|6|Mentioned|P13||Archean|Age of unit is 2640+/-8 Ma||||||07-NOV-08
34585|Clark Well Monzogranite|50075|5|Briefly described|p16|Archean|Archean|Age: 2640 +/- 8 Ma (U-Pb) Nelson, 1996. Geological Province: Yilgarn Craton.||||||07-NOV-08
34585|Clark Well Monzogranite|60076|5|Briefly described|p45 App. 1|||[Agmcw]   Biotite bearing, seriate grain size.||||||
34585|Clark Well Monzogranite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Seriate, biotite-bearing monzogranite.||||||07-FEB-11
34585|Clark Well Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Seriate, biotite-bearing monzogranite.|05-AUG-15
34585|Clark Well Monzogranite|69631|5|Briefly described|p34|Neoarchean|Neoarchean|This age dates the last movement on the Ida Fault.|2640 +/- 8 Ma (Nelson, 1996).l|||||
34585|Clark Well Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Seriate, biotite-bearing monzogranite.|
34585|Clark Well Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
34585|Clark Well Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. See 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|||||Seriate, biotite-bearing monzogranite|
77935|Claudius Member|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2662 - 2640 Ma (inferred).|Scotty Creek Formation|||Polymictic conglomerate and minor interbedded sandstone; metamorphosed.|
77935|Claudius Member|70326|5|Briefly described|p339|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton.||Unit of Scotty Creek Formation.||Locally underlain unconformably by Agnew Komatiite, Redeemer Basalt and Burrell Well Basalt.||
77935|Claudius Member|71212|5|Briefly described|intro p2, intro p3|||Yilgarn Craton. ||Scotty Creek Formation||Overlies the Agnew Komatiite.|Polymictic conglomerate.|
77935|Claudius Member|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2662-2640 Ma (inferred)|Unit of Scotty Creek Formation.|||Polymictic conglomerate and minor interbedded sandstone; metamorphosed|
77935|Claudius Member|73151|5|Briefly described|p2, p13|Neoarchean|Neoarchean|Yilgarn Craton, Kalgoorlie Terrane.||Scotty Creek Formation|||Conglomerate dominated by rounded basalt and komatiite clasts at the base, becomes progressively enriched in tonalitic clasts up-sequence. The conglomerate is massive, poorly sorted, clast-supported and contains a sandy matrix.|
80172|Cleghorne Formation|71211|4|Described|p26-p36, p47|Stenian|Stenian|Up to 100m thick. Lithofacies discussed in detail. On p30 subdivided into an Upper and Lower Formation. Deposited in a shallow sub-tidal environment that was above storm-wave base (on the basis of hummocky cross stratification). See also  p48 fig 2.11, p56, p60-p64, p66, p86, p87 fig 3.2, p135, p138, p208, p216, 265. Age inferred from surrounding units.||||Conformably overlies the Mount Palgrave Group. Overlain by the Kathleen Ignimbrite and the Glyde Formation. Intruded by the Rowland Suite.|Mudstone, conglomerate, basalt, breccias and quartz-feldspar sandstones.|03-OCT-17
68665|Cleland Supersuite|61253|5|Briefly described|p52 Fig. 2, p58|Archean|Archean| Age: ~3.27-3.24Ga.   Geological Province: Pilbara Craton. See also p54-55 Fig. 3.||||||07-NOV-08
68665|Cleland Supersuite|63417|5|Briefly described|Map legend|Archean|Archean|Includes Little River Trondhjemite, Midgengadgi, Bullgarina and Bishop Creek Monzogranites. Age: 3246-3241Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
68665|Cleland Supersuite|63420|5|Briefly described|Map legend|Archean|Archean|Includes the Wolline Monzogranite.  Ages include c.3252Ma and c.3250Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
68665|Cleland Supersuite|63441|4|Described|p35, p9 Tb. 2, p31 Fig. 10|Archean|Archean|Includes Bishop Creek, Bullgarina, Strelley and Wolline Monzogranites; Kavir, Siffleetes and Karratha Granodiorites + Tarlwa Pool Tonalite; Strelley is the  type granite. Age: 3275-3225Ma. Geol.prov: Pilbara Craton. Monzogranite, tonalite to granodiorite.||||||07-FEB-11
68665|Cleland Supersuite|63538|6|Mentioned|p5, p6 Fig. 3|Archean|Archean|Geological Province: Pilbara Craton.||||||19-APR-13
68665|Cleland Supersuite|64174|5|Briefly described|Map legend|Archean|Archean|Includes Karratha Granodiorite and Tarlwa Pool Tonalite.  Age range includes: 3270-3261Ma and c.3236Ma. Geological province: Karratha Terrane, West Pilbara Superterrane.||||||17-MAR-09
68665|Cleland Supersuite|64580|6|Mentioned|map legend|||||||||
68665|Cleland Supersuite|64621|5|Briefly described|Map legend|Archean|Archean|Includes Bishop Creek Monzogranite. Age: 3246-3220Ma.||||||07-NOV-08
68665|Cleland Supersuite|64657|5|Briefly described|Map Legend|Archaean|Archaean|Includes Kavir Granodiorite. Geological Province: Pilbara Craton.||||||
68665|Cleland Supersuite|64662|5|Briefly described|p44|Archean|Archean|Age: ~3.27 - 3.23Ga. Geological Province: western Pilbara Craton. Possible source rocks for Ferdies Member, Dead Bullock Formation, Tanami region.||||||07-FEB-11
68665|Cleland Supersuite|65724|5|Briefly described|map legend|Paleoarchaean|Paleoarchaean|Under Kylena Fm; intruded by Elsie Creek Tonolite. 2 unnamed units: biotite monzogranite (age: c. 3275 Ma, geochron. S. Bodorkos in prep);and, quartz-biotite trondjhemite and tonalite. Geol. Prov: East Pilbara Granite-Greenstone Terrane.||||||
68665|Cleland Supersuite|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. This name replaces that part of the Mount Edgar Granitoid Complex, in Version 1 of this map sheet (see Refid 65726), which included these two units.|c.3240 Ma.||Includes Bullgarina and Bishop Creek Monzogranites.|||
68665|Cleland Supersuite|65827|3|Fully described|p6 Tb.2, p15-16, p26, p57|Paleoarchean|Paleoarchean|Of Mount Edgar Granitic Complex; 3275-3225 Ma. Includes Bishop Creek and Bullgarina Monzogranites. Intruded by Split Rock Supersuite; intrudes Emu Pool Supersuite. Weakly foliated, massive monzogranite, granodiorite and syenogranite intrusions.||||||
68665|Cleland Supersuite|65829|3|Fully described|p1, p7 Fig.3, p10, pp12-13. |Paleoarchean|Paleoarchean|These intrusives are widely separated, small (<4 km2) stocks and microgranitic dykes. Their intrusion into the Yilgalong Granitic Complex is the last event in the East Pilbara Terrane (in this map area), and was followed by c.500 m.y. gap representing erosion and weathering, prior to Hamersley Basin deposition of the Fortescue Group.|3275 - 3225 Ma.||Includes Midgengadgi Monzogranite and Little River Trondhjemite.|Intrudes Yilgalong Granitic Complex.|Biotite monzogranite, unfoliated, seriate to porphyritic, leucocratic; leucocratic trondhjemite, massive, fine- to medium-grained, albitized, undeformed; weakly foliated biotite tonalite; dykes of porphyritic microgranodiorite and micromonzogranite.|
68665|Cleland Supersuite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Unit of Pilbara Supergroup. Includes Bishop Creek, Strelley and Garden Creek Monzogranites; Siffleetes and Kavir Granodiorites; and unnamed units of tonalitic orthogneiss, monzogranite, granodiorite and tonalite.||||||
68665|Cleland Supersuite|66217|4|Described|p1, p5, p6 Table 1, pp9-11, pp33-35. |Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Predominantly potassic. Derived from partial melting of older supersuites, and emplaced during episodes of partial convective overturn of the upper and middle crust, contemporaneous with eruption of the Sulphur Springs Group.|3275-3225 Ma.|Unit in Carlindi Granitoid and Mount Edgar Granitic Complexes.|Includes Wolline, Strelley and Bishop Creek Monzogranites; Karratha Granodiorite.||Strongly foliated and folded granitic rocks: monzogranite, foliated monzogranite, tonalite, granodiorite.|
68665|Cleland Supersuite|67201|4|Described|p7 Fig.4, p11, p14, p16-17 Fig.9, p26|Archean|Archean|West Pilbara Superterrane and East Pilbara Terrane. Youngest granitic supersuite in East Pilbara Terrane. Age: most dated intrusions are 3250-3230 Ma, and earlier c.3275-3260 Ma suite.|||Karratha Granodiorite, Tarlwa Pool Tonalite|||
68665|Cleland Supersuite|68035|5|Briefly described|p286 Fig 3|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Associated with Sulphur Springs Group.|3.27 - 3.23 Ga|||||
68665|Cleland Supersuite|68280|6|Mentioned|p3|Paleoarchean|Paleoarchean||3270-3230 Ma|||||
68665|Cleland Supersuite|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|Pilbara Craton.|c.3252 Ma.||||Mylonitic metamonzogranite; hornblende-porphyritic monzogranite, medium grained, foliated, metamorphosed.|02-DEC-14
68665|Cleland Supersuite|68282|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|3240-3220 Ma||Includes Garden Creek Monzogranite, Kavir Granodiorite.|||
68665|Cleland Supersuite|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. An un-named sub-unit has an age of c.3252 Ma.|c.3250 Ma||Includes Wolline Monzogranite.||Granitic rock, medium to coarse grained, massive to foliated, metamorphosed; monzogranite grading to syenogranite; hornblende-porphyritic monzogranite.|06-JAN-15
68665|Cleland Supersuite|69013|5|Briefly described|Map Legend|Mesoarchean|Paleoarchean|East Pilbara Terrane. 3 unnamed facies are mapped separately. Contains minor banded granitic gneiss of the Callina Supersuite.|||Includes Kavir Granodiorite and Siffleetes Granodiorite.||Includes mixed metagranitic rock; minor banded granitic gneiss; pegmatite, monzogranite, greenstone, granite dykes; mixed granite, gneiss, and leucogranite; meta biotite granodiorite, minor pegmatitic granite; meta biotite-hornblende granodiorite.|29-APR-14
68665|Cleland Supersuite|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.  Includes units dated by Buick et al (2002) in the range: 3239-3238 Ma. See map legend for a detailed lithological description.|c.3240-c.3238 Ma.||Includes the Strelley Monzogranite and the Kavir Granodiorite.||Includes monzogranites; microdiorite and diorite; dolerite and gabbro; biotite granodiorite; all metamorphosed.|02-MAY-14
68665|Cleland Supersuite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Also includes tonalitic orthogneiss.|||Includes Kavir Granodiorite, Wolline Monzogranite, Bishop Creek Monzogranite, Bullgarina Monzogranite, Garden Creek Monzogranite, Siffleetes Granodiorite, Strelley Monzogranite||Tonalite and granodiorite; metamorposed. Metamonzogranite, metagranodiorite, metadiorite and metatonalite. Biotite monzogranite, pegmatite quartz-biotite trondhjemite and tonalite, mixed granite, gneiss and leucogranite with abundant xenoliths.|
68665|Cleland Supersuite|69185|5|Briefly described|500k_geologyp08_lut.csv|||Geological Province: Pilbara Craton.|||Includes Karratha Granodiorite, Strelley Monzogranite, Tarlwa Pool Tonalite.|||
68665|Cleland Supersuite|69301|5|Briefly described|p5 Fig.3, p8|||Pilbara Craton. West Pilbara Superterrane and East Pilbara Terrane. Pilbara Supergroup successions include thick felsic volcanic formations, each contemporaneous with the four granitic supersuites. i.e. Kangaroo Caves and Cleland Supersuite.|||||Granitic rocks.|
68665|Cleland Supersuite|69566|6|Mentioned|p236|||Mount Edgar Granitoid Complex, East Pilbara Granite-Greenstone Terrane.|3275-3225 Ma.||Bishop Creek Monzogranite.|||
68665|Cleland Supersuite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|3252-3224 Ma (inferred)||Includes Bishop Creek Monzogranite, Bullgarina Monzogranite, Garden Creek Monzogranite, Kavir Granodiorite, Siffleetes Granodiorite, Strelley Monzogranite, Wolline Monzogranite.||Monzogranite and metamonzogranite, metadiorite, granodiorite and metagranodiorite, tonalite, banded granitic gneiss|
68665|Cleland Supersuite|70022|6|Mentioned|p115-116|||Pilbara Craton.|||Wolline Monzogranite.|||
68665|Cleland Supersuite|70775|5|Briefly described|p8 fig 5, p9, |Paleoarchean|Paleoarchean|Karratha Terrane. See also p15-p17, p19, p23-p24, p44 fig 27, p68|c. 3274-3223 Ma||Includes the Karratha Granodiorite and the Tarlwa Pool Tonalite.|||
68665|Cleland Supersuite|70826|6|Mentioned|p8|||||||Intrudes Sulphur Springs Group, Roebourne Group.  Unconformably overlain by Nickol River Formation.||13-MAY-20
68665|Cleland Supersuite|70884|6|Mentioned|p122-123|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|3.28-3.22 Ga|||||
68665|Cleland Supersuite|71041|6|Mentioned|p44, 42||||3275-3225 Ma||||Granitoid rocks.|08-NOV-17
68665|Cleland Supersuite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite, granodiorite, monzogranite, pegmatite|
68665|Cleland Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Subdivided into 9 named and 1 unnamed unit.|Max age 3274+/-5 ma, min 3223+/-3 Ma.||Includes Bishop Creek Monzogranite, Strelley Monzogranite, Wolline Monzogranite, Garden Creek Monzogranite,  Bullgarina Monzogranite, Tarlwa Pool Tonalite, Kavir, Karratha, Siffleetes Granodiorites.||Monzogranite, granodiorite, and tonalite; local gabbro and dolerite; variably metamorphosed. Tonalitic orthogneiss; locally includes veins of granitic pegmatite or greenstone xenoliths.|
68665|Cleland Supersuite|72064|6|Mentioned|p79|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Overlaps in age with Paleoarchean zircons found in the Strelley Pool Formation.|c. 3.27-3.22 Ga|||||
68665|Cleland Supersuite|72251|5|Briefly described|p52-54,65|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane and West Pilbara Superterrane, Pilbara Craton. Granitic supersuite with Nd model age of ~4.1-3.4 Ga (Smithies et al., 2003, 2007; Champion, 2013).|3.25-3.22 Ga||||Monzogranite and syenogranite.|
68665|Cleland Supersuite|72668|5|Briefly described|p4, p6, p9, p11, p13-14, p19, p27-28|||West Pilbara Superterrane. Form the oldest granitic rocks in the West Pilbara Superterrane. Synchronous with the D4 deformation.|c. 3275-3225 Ma|||Coeval with the Roebourne Group.|Dominantly monzogranites. Compositions range from trondhjemite to diorite to syenite.|12-JAN-22
68665|Cleland Supersuite|73160|6|Mentioned|p12|Paleoarchean|Paleoarchean||3.27-3.22 Ga||||Felsic intrusions.|
68665|Cleland Supersuite|73598|6|Mentioned|p1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.||||||
78609|Clianthus Flat Rhyodacite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2692 - 2655 Ma (inferred).|Black Flag Group|||Rhyodacite to dacite; coherent lava with minor dacitic volcaniclastic sandstone and breccia; metamorphosed.|
78609|Clianthus Flat Rhyodacite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2692-2655 Ma (inferred)|Unit of Black Flag Group.|||Rhyodacite to dacite; coherent lava with minor dacitic volcaniclastic sandstone and breccia; metamorphosed|
31467|Clianthus Formation|23523|5|Briefly described|p995|Early Permian|Early Permian|Of Grant Group. Geological Province: Canning Basin.||||||
31467|Clianthus Formation|43823|4|Described|p754|||||||||
31467|Clianthus Formation|64580|6|Mentioned|map legend|||Of Grant Group.||||||24-NOV-08
31467|Clianthus Formation|64630|5|Briefly described|p31 Fig.2, p35|Sakmarian|Sakmarian|N.B. Tentative ages, awaiting further palynology work. Province: subsurface Barbwire Terrace area of Canning Basin. Part of the Grant Group, underlies the Poole Sandstone, overlies the Calytrix Formation. Palynology age: P. confluens.||||||28-OCT-09
31467|Clianthus Formation|64643|5|Briefly described|p8|Sakmarian|Sakmarian|Of Grant Group across the Barbwire Terrace.||||||24-NOV-08
31467|Clianthus Formation|64971|5|Briefly described|p684, p685 Fig. 2|Early Permian|Early Permian|Of Grant Group. Geological Province: Canning Basin.||||||09-FEB-10
31467|Clianthus Formation|66949|4|Described| p18-20p10, p13-14,; p46-48,51-54 Appx.2|Sakmarian|Sakmarian|See also p58 Appx.3, p60-65 Appx.4; p66-71,75,78,82,93 Appx.5; Plates 8-10,12. Type section in Pratia 1detailed. Up to 170m thick; deltaic to fluvial deposits. No glacial influence in type area (Barbwire Terrace). Contains brachiopods, forams. It is also stated that the unit contains no evidence of marine influence [brachiopods?] and that woody material is common throughout, thus resembling Millajiddee member. Available core and Formation picks detailed.||Upper unit in Grant Group on Barbwire Terrace.||Conformably overlies Calytrix Formation. Is overlain by Poole Sandstone.|Sandstone, minor siltstone.|30-OCT-15
31467|Clianthus Formation|67354|6|Mentioned|p108 Fig.39.|||||||Overlies Calytrix Formation. Is overlain by Poole Sandstone.||
31467|Clianthus Formation|68007|5|Briefly described|p9|Permian|Permian|||Grant Group.||Equivalent to Carolyn Formation.||
31467|Clianthus Formation|68656|6|Mentioned|GEOL_LUT_CSV/500k_geologyp08_lut|||||Grant Group||||
31467|Clianthus Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Cisuralian|Pennsylvanian|||||||
31467|Clianthus Formation|69297|6|Mentioned|p337, p352|Sakmarian|Sakmarian|Broome Platform of the Canning Basin. ||Grant Group||Overlies the Calytrix Formation. Overlain by the Nura Nura Member.||
31467|Clianthus Formation|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Grant Group.||||
31467|Clianthus Formation|69693|5|Briefly described|p3-4, 10|Sakmarian|Sakmarian|Barbwire Terrace, Canning Basin. A post-glacial sequence deposited in a deltaic to fluvial environment. Is also mis-spelled as Clianthys Fm. on p3.||Grant Group||Overlies Calytrix Formation. Equivalent to Carolyn Formation.|Sandstone and mudstone.|
31467|Clianthus Formation|70774|5|Briefly described|p5 fig 3|Sakmarian|Sakmarian|Canning Basin.||Grant Group||Overlies the Calytrix Formation. Overlain by the Nura Nura Member (Poole Sandstone).||
31467|Clianthus Formation|72496|5|Briefly described|p217-218, 220, p230-231|Sakmarian|Sakmarian|Canning Basin, Barbwire Terrace. Interpreted to represent post-glacial deltaic to fluvial deposition.||Grant Group||Equivalent to the Carolyn Formation. Overlies the Calytrix Formation.||19-MAR-20
31467|Clianthus Formation|72497|5|Briefly described|p4.|Permian|Permian|After Redfern and Millward, 1994. Recognised in subsurface Barbwire Terrace area. Implied to be part equivalent to upper Carolyn Formation.||upper Grant Group||Shown as overlying Calytrix Formation.||
31467|Clianthus Formation|73117|4|Described|p15, p22, p24-26, p28, p111-113, p117|Asselian|Asselian|Name proposed by Redfern (1991) as an alternative subdivision of the Grant Group to that of Of Crowe and Towner (1975). Name derived from a well at the south-eastern end of the Barbwire Terrace. This scheme for constituents of the Grant Group has been applied inconsistently across the Barbwire Terrace. Proposed lectostratotype section from Pratia 1 well (Apak and Backhouse, 1999). Includes the P. confluens Zone.||Grant Group||Underlain[?] by Calytrix Formation. Overlain[?] by Poole Sandstone and Noonkanbah Formation.|Fluvio-deltaic sandy facies.|
68503|Cliff Pool Tonalite|63441|2|Defined|p10 Tb. 2, p36|Archean|Archean|Of Elizabeth Hill Supersuite, in Cherratta Granitic Complex. Age: 3068+/-4Ma. Unconformable below Hardey Fm. Intrudes Pinnacle Hill Gneiss; intruded by Munni Munni Intrusion. Geol.prov: West Pilbara Superterrane/Pilbara Craton. Foliated biotite tonalite.||||||07-FEB-11
68503|Cliff Pool Tonalite|64174|5|Briefly described|Map legend|Archean|Archean|Within the Elizabeth Supersuite. Age: c.3068Ma. Weakly foliated to gneissic biotite tonalite; metamorphosed.||||||07-NOV-08
68503|Cliff Pool Tonalite|64580|4|Described|map legend||Mesoarchean|Of Elizabeth Hill Supersuite. Weakly foliated to gneissic biotite tonalite; metamorphosed.||||||15-DEC-08
68503|Cliff Pool Tonalite|67201|4|Described|p19|||In west Pilbara. Outcrops over 70 km2, as part of Cherratta Granitic Complex east of Munni Munni Intrusion.|3068+/-4 Ma (Nelson 1998)|Elizabeth Hill Supersuite.||Intrudes Pinnacle Hill Gneiss (Railway Supersuite). Southern contact is intruded by Maitland River Supersuite.|Foliated biotite tonalite.|22-NOV-16
68503|Cliff Pool Tonalite|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Elizabeth Hill Supersuite.|||Weakly foliated to gneissic biotite tonalite; metamorphosed|
68503|Cliff Pool Tonalite|70775|5|Briefly described|p25 tbl 4, p38, p66|Mesoarchean|Mesoarchean|Also dated at 3068 Ma (Nelson, 1998m)|c. 3070 Ma (Smithies et al., 2007a)|Elizabeth Hill Supersuite||Intrudes the Pinnacle Hill Gneiss. Intruded by the Maitland River Supersuite.||
68503|Cliff Pool Tonalite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||tonalite|
68503|Cliff Pool Tonalite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||3068+/-4 Ma.|Elizabeth Hill Supersuite|||Weakly foliated to gneissic biotite metatonalite.|
81375|Cliffs Ultramafic|70326|4|Described|p360,364-365|Neoarchean|Neoarchean|Geological province: Boorara Domain North, Kalgoorlie Terrane, Yilgarn Craton. Produced during ~2705 Ma komatiite eruption event. |~2705 Ma|||Underlain by Centenary Bore Basalt. Correlable to Agnew and Siberia Komatiites, and Hampton Formation.|Spinifex-textured komatiite with comagmatic dacite intrusions.|
29482|Clifton Downs Member|63454|4|Described|p71 Tb. 2, p75|Pleistocene|Pleistocene|Lower to middle part of Tims Thicket Limestone. White to cream shelly/bioturbated calcarenite, bioturbated forameniferal limestone, laminated x-laminated marine calcarenite, laminated to x-laminated beach calcarenite.||||||08-AUG-07
32215|Cloisters Member|23755|5|Briefly described|p34|Archean|Archean|Of Euro Basalt. Max. thickness: 2700 m.||||||07-NOV-08
32215|Cloisters Member|61266|5|Briefly described|p57|Archean|Archean|Of the Euro Basalt. Spinifex-textured, massive and pillowed ultramafic lavas and pillowed high-Mg basalt. Overlain by the Miralga Creek Member. Geological Province: Pilbara Craton.||||||07-NOV-08
41037|Clover Downs beds|24196|6|Mentioned|p69 Fig.10|||Geological Province: East Agnew-Mount Clifford sub-basin, Yilgarn Craton.||||||
24851|Clutterbuck Formation|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
24851|Clutterbuck Formation|41751|6|Mentioned|p8|||||||||
24851|Clutterbuck Formation|64580|4|Described|map legend||Neoproterozoic|Feldspathic sandstone, siltstone, and conglomerate.||||||09-DEC-08
24851|Clutterbuck Formation|65102|6|Mentioned|p368|Neoproterozoic|Neoproterozoic|Now considered part of Amadeus Basin.  Tentatively correlated with Punkerri and Wirrildar Formations.||||||
24851|Clutterbuck Formation|67856|4|Described|p340, 338, 335, 337, 344, 345, 346|Neoproterozoic|Neoproterozoic|Of Jackson & van de Graff (1981). Type section: main range of Clutterbuck Hills. 4.5m [p345] or 4500m [p340] thick marine sediments. No age determination. Isolated sequence in extreme west of Amadeus Basin. Lithologically similar to Punkerri and Wirrildar Formations of Officer Basin. Could possibly correlate with Julie Formation, Arumbera Sandstone.||||Relationships uncertain. Unconformably overlain by Permian.|Cross-bedded feldspathic arenite; siltstone and conglomerate interbeds. Thin beds of carbonate, calcarenite, shale near base.|
24851|Clutterbuck Formation|69182|6|Mentioned|Ch4 p3|||Canning Basin. ||||||
24851|Clutterbuck Formation|70793|4|Described|500k_interpgeop14_lut.csv|Series 2|Ediacaran|Of Amadeus Basin (Phase 1), Centralian Superbasin. Events: Areyonga Movement; Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma).|635-509 Ma (inferred)||||Fine- to coarse-grained feldspathic sandstone, conglomerate and siltstone interbeds|
24851|Clutterbuck Formation|70826|6|Mentioned|p5 tbl 2|||Supersequence 4, Centralian Superbasin.||||||20-APR-20
24851|Clutterbuck Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, conglomerate, sandstone|
24851|Clutterbuck Formation|71268|4|Described|GEOL_LUT_CSV files|Series 2|Ediacaran|Of Amadeus Basin (Phase 1), Centralian Superbasin. Events: Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma). See 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|635-510 Ma (inferred)||||Fine to coarse well sorted cross-bedded feldspathic sandstone with siltstone and conglomerate interbeds|
24851|Clutterbuck Formation|72034|5|Briefly described|500k_interpgeop16_lut|Series 2|Ediacaran|Amadeus Basin (Phase 1).|||||Fine- to coarse-grained feldspathic sandstone, conglomerate and siltstone interbeds.|
79343|Cobb Formation|71268|4|Described|GEOL_LUT_CSV files|Ordovician|Ordovician|Of Cobb Embayment, Canning Basin. Events: Western Australian events (4000-0.01 Ma). See 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|485.4-443.4 Ma (inferred; biostrat)||||Sandstone, siltstone, conglomerate; minor local dolostone|
79343|Cobb Formation|72094|5|Briefly described|p3 Fig 2, p15-16 Fig 11|Ordovician|Ordovician|Cobb Embayment, Canning Basin. See also Cobb Embayment discussion p7.||||Unconformably overlies Warakurna Supersuite, Kunmarnara Group.||
79343|Cobb Formation|73117|5|Briefly described|p3|Llandovery|Middle Ordovician|Canning Basin.||||Underlain by Goldwyer Formation. Overlain by Worral Formation. Equivalent to Carribuddy Group and Nita Formation.|Dominantly sandstone with lesser conglomerate.|
79343|Cobb Formation|73346|2|Defined|p1-2, p5, p7, p9-28, p30, App.1, App.3|Darriwilian|Tremadocian|New name [article includes definition card]. Canning Basin, Cobb Embayment; unit named after this basin subdivision / Lake Cobb. Constitutes the main exposed stratigraphic unit in the embayment; represents only the third known surface exposure of Ordovician rocks in the Canning Basin. Type area encompasses a sparse cluster of small hills located 22-30 km east to east-northeast of Wanarn Community; includes three short reference sections that are likely to be laterally correlative. Thickness is poorly understood; 20-30 m maximum outcrop thickness at any one site, >122 m thick in a water bore, and up to 800 m thick (thinning eastwards) in seismic interpretations. Regionally variable lithology. Deposition occurred in alluvial fan, fluvial and marginal marine environments (apparently restricted; lagoonal, estuarine and locally evaporitic), opening westward into the main basin. Halite pseudomorphs indicate periodic evaporitic conditions. Abundant fragmentary fish fossils and trace fossils observed at the type area but not elsewhere; these provide broad age constraint but the base of the unit could be considerably older. Numeric age is a single grain detrital zircon maximum depositional age (1 sigma). Unit is not prospective for hydrocarbons at the type area but western lateral equivalents could be (e.g., in the subsurface on the Ryan Shelf?). Broadly similar in age to the Stairway Sandstone. Unconformably overlies very weathered granite of Musgrave region basement. May be equivalent to the Nambeet (upper part), Willara, Goldwyer or Nita formations or lower poriton of the Carribuddy Group.|478 +/- 7 Ma U-Pb SHRIMP|||Unconformably overlain by Grant Group.|Predominantly fine- to coarse-grained red-brown sandstone, pebbly sandstone, and minor local conglomerate with recessive intervals of siltstone and rare thin carbonate interbeds. Common phosphate nodules in the type area.|
79343|Cobb Formation|73437|6|Mentioned|p151|Paleozoic|Paleozoic|Canning Basin, Cobb Embayment.||||||
67829|Coburn Formation|6943|5|Briefly described|p599, pp601-603, pp605-606, p608.|Late Silurian|Silurian|Replaced (Mory et al. 1998) the name Hamelin Formation, and excluded that unit's evaporite part, the Yaringa Formation. Up to 335 m thick. Algal, carbonate-rich potential hydrocarbon source.||Uppermost unit in Dirk Hartog Group. ||Overlies Yaringa Formation, probably paraconformably. Overlies Marron Member of Ajana Formation disconformably in BHP ND 002. Unconformably overlain by Nannyarra and Faure Formations.||
67829|Coburn Formation|12729|4|Described|p.5, 8, 10-1, 28; Figs. 8, 9|Late Silurian||Replaces the name 'Hamelin Formation' of Gorter et al. (1994). Type section 947 - 1194.8 m in Yaringa 1 (modified by Mory et al. 1998 after Gorter et al. 1994). Conodont fauna, Ozarkodina confluens, (late Early to latest Silurian) observed. Intersections up to 335 m.||Dirk Hartog Group||Conformably overlies the Yaringa Formation; disconformably overlies Marron Member (Ajana Formation). Unconformably overlain by the Nannyarra Formation.|Consists mainly of dolomitic carbonate, contains thin, organic-rich shale beds.|17-SEP-15
67829|Coburn Formation|12731|6|Mentioned|p596.|Silurian|Silurian|||Unit in Dirk Hartog Group.|||Includes thin organic-rich shale beds.|
67829|Coburn Formation|14228|5|Briefly described|p1, p4-6, p15-16, p19, p26 |Late Silurian|Early Silurian|Gascoyne Platform. Petroleum source beds. Maturity of oil rises to north.||Dirk Hartog Group||Overlies Yaringa Formation.|Light-grey dolostone, skeletal debris, ooids, gypsiferous, gypsum veins.|
67829|Coburn Formation|23572|4|Described|p10|Silurian|Silurian|Geological Province: Carnarvon Basin. Of the Dirk Hartog Group. Underlying Unit: Yarringa Formation. Max. thickness: 335m||||||12-MAY-05
67829|Coburn Formation|23935|4|Described|p11 Fig.7, p19|Pridoli|Ludlow|Of Dirk Hartog Group. Conformably overlies Yaringa Formation. Unconformably overlain by Faure Formation. Interbedded dolomite and gypsum, with minor shale. Thickness: 18 m. Geological Province: Southern Carnarvon Basin.||||Replaces Hamelin Formation of Gorter et al. (1994)||23-SEP-15
67829|Coburn Formation|49942|4|Described|p4 Fig.3, p9|Pridoli|Wenlock|Conformably overlies Yaringa Formation. Of Dirk Hartog Group. Evaporitic and carbonate-siliclastic sediments. Geological Province: Gascoyne Platform.||||||
67829|Coburn Formation|50084|4|Described|p77, 78|Silurian|Silurian|Overlies Yaringa Formation (disconformably) and Ajana Formation. Overlain by Faure Formation following a hiatus. Thickness: 213.5 m.Of Dirk Hartog Group. Geological Province: Southern Carnarvon Basin.||||||07-FEB-11
67829|Coburn Formation|60384|6|Mentioned|p243 Fig 2a|Pridoli|Wenlock|||Of Dirk Hartog Group||||
67829|Coburn Formation|60725|5|Briefly described|p28, p29 Fig.2, p30, p34, p36, p39|Silurian|Silurian|Locally, moderate to good petroleum source potential. Early stages of oil generation.||Unit in Dirk Hartog Group.|||Carbonate-shales facies.|
67829|Coburn Formation|61560|6|Mentioned|p493|Silurian|Silurian|||||||
67829|Coburn Formation|61562|5|Briefly described|p547|Late Silurian|Late Silurian|||||||
67829|Coburn Formation|65449|5|Briefly described|p34|||Southern Carnarvon Basin.||Dirk Hartog Group.|||Dominated by dolomitic carbonate.|
67829|Coburn Formation|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.||Dirk Hartog Group|||Includes blue/grey (light and dark laminations) dolomitic claystone.|
67829|Coburn Formation|67200|6|Mentioned|p18 table 1, p46, p52, p56, app 2 p4|||Thermal conductivity of 2.59 W/mK||Dirk Hartog Group|||Dolomitic claystone.|
67829|Coburn Formation|69297|6|Mentioned|p246, p249, p250|Silurian|Ordovician|Gascoyne Sub-basin of the Carnarvon Basin. Oil staining and fluorescence were detected have been detected in this unit. This unit is one of the primary candidate source rocks in the Gascoyne Sub-basin. ||Dirk Hartog Group||Overlies the Yaringa Formation. Overlain by the Faure Formation.||
67829|Coburn Formation|71146|5|Briefly described|p6|Pridoli|Wenlock|Southern Carnarvon Basin.||Dirk Hartog Group||Overlies the Yaringa Formation. Disconformably overlain by the Faure Formation.|Carbonate and mudstone.|
73776|Cocanarup pegmatites|50542|5|Briefly described|p125|||Informal name. Hosted by Annabelle Volcanics. Gological Province: Yilgarn Craton.||||||07-FEB-11
79565|Cock Robin Formation|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2817-2753 Ma (inferred)||||Fuchsite-quartz-andalusite schist, tremolite-chlorite(-talc) schist, amphibolite and mafic schist; locally garnetiferous, banded and pyritic chert; local banded iron-formation; metamorphosed, silicified slate, basalt; metamorphosed.|
79565|Cock Robin Formation|73596|6|Mentioned|p1159, 1162, 1164|Neoarchean|Mesoarchean|Broad Arrow Inlier, Kalgoorlie Terrane.|2804 +/- 6 Ma (Wingate et al., 2022).|||Is overlain by Scotia Basalt (Broad Arrow Subgroup).||
39607|Cockeraga Leucogranite|24533|4|Described|p4 Table 1, 7|Archean|Archean|Of the Yule Granitoid Complex. Comprises leucocratic biotite (-hornblende) tonalite or granodiorite, with subordinate monzogranite; Age: < 3068 +/- 22 Ma and < 3066 +/- 4 Ma (SHRIMP).||||||15-APR-13
39607|Cockeraga Leucogranite|24534|5|Briefly described|Map legend|Archean|Archean|Of the Yule Granitoid Complex. Age: 2935Ma.||||||15-APR-13
39607|Cockeraga Leucogranite|24554|4|Described|p5 Tb.1, p8|Archean|Archean|Of the Yule Granitoid Complex. Age: c. 3065 Ma. Geological Province: East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
39607|Cockeraga Leucogranite|50146|5|Briefly described|Map Legend|Archean|Archean|Of the Yule Granitoid Complex. Age: <3065 Ma. Geological Province: Pilbara Craton. Leucocratic biotite (-hornblende) tonalite and granodiorite and subordinate monzogranite; locally abundant pegmatite, and greenstone and granitoid gneiss xenoliths.||||||07-NOV-08
39607|Cockeraga Leucogranite|63372|4|Described|Map Legend|Archean|Archean|Of the Yule Granitoid Complex. Geological Province: East Pilbara Granite-Greenstone Terrane.  Age: 3066-2940 Ma. Leucocratic biotite(-hornblende) tonalite and granodiorite and subordinate monzogranite; well-developed schlieric banding;||||||15-APR-13
39607|Cockeraga Leucogranite|63441|5|Briefly described|p10 Tb. 2, p36|Archean|Archean|Of Elizabeth Hill Supersuite (in Yule Granitic Complex). Ages: 3068 +/- 22 Ma and 3066 +/- 4 Ma. Geological Province: East Pilbara Terrane/Pilbara Craton. Characterised by schlieric texture in biotite(-hornblende) tonalite or granodiorite with rare monzogranite||||||15-APR-13
39607|Cockeraga Leucogranite|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Unit in Elizabeth Hill Supersuite. 3068-3066 Ma. Leucocratic biotite(-hornblende) tonalite, granodiorite and subordinate monzogranite; local pegmatite, and greenstone and granitic gneiss xenoliths; weakly metamorphosed. ||||||
39607|Cockeraga Leucogranite|66118|4|Described|p157|||Occurs in southern central part of Yule Granitic Complex.|c. 3068 Ma|Yule Granitic Complex|||Dark grey, medium- and even-grained foliated diorite phase that occurs as rafts and xenoliths (contains inherited zircons).|
39607|Cockeraga Leucogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|Age derived from diorite samples (169014.1.pdf, 169016.1.pdf)|3068 +/- 22 Ma (SHRIMP) 3066 +/-4 Ma (SHRIMP)|Elizabeth Hill Supersuite|||Leucocratic biotite(--hornblende) tonalite, granodiorite and subordinate monzogranite with well-developed schlieric banding; local pegmatite, and greenstone and granitic gneiss xenoliths; weakly metamorphosed|
39607|Cockeraga Leucogranite|69590|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Prinsep Orogeny. Sample GSWA 169014 (bt-hbl quartz diorite) yielded an interpreted igneous crystallisation age of 3068+\-22 Ma for the diorite (weighted mean 207Pb/206Pb). Sample GSWA 169016 (leucocratic biotite quartz diorite) yielded an interpreted maximum igneous crystallisation age of 3066+\-4 Ma for the diorite (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv.|3068-3066 Ma (isotopic)|Unit of Elizabeth Hill Supersuite.|||Leucocratic biotite(-hornblende) tonalite, granodiorite and subordinate monzogranite; well developed schlieren banding, local pegmatite, and greenstone and granitic gneiss xenoliths; weakly metamorphosed|
39607|Cockeraga Leucogranite|70775|5|Briefly described|p38|||Also dated at 3068 +/- 22 Ma (Nelson, 2002a).|3066 +/- 4 Ma (Nelson, 2002b)|||||
39607|Cockeraga Leucogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||tonalite, granodiorite, monzogranite, pegmatite|
39607|Cockeraga Leucogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||Max age 3068+/-4 Ma, min 3066+/-22 Ma|Elizabeth Hill Supersuite|||Leucocratic biotite(--hornblende) tonalite, granodiorite and subordinate monzogranite; local pegmatite, and greenstone and granitic gneiss xenoliths; weakly metamorphosed.|
80522|Cody Limestone|13615|3|Fully described|p4, p6-8, p41-42, p48, 83, 103 App.3|Late Permian|Late Permian|Peedamullah Shelf.  Up to 70m thick. Spores and Pollen zone provided. Intersected by Abdul's Dam 1 drillhole. The type section occurs in Cody 1 drillhole between 3000 to 3088m. Contains microfossils and fragments of brachiopods and byrozoans. Deposited in a marine shelf environment.  Previously called Wandagee Formation in Ruby 1 (Mills, 1997), Wandagee Limestone in Abdul's Dam 1. See also p17, 62,  85, p119 App. 5,  Plates 2, 3.||Of Kennedy Group.||Conformable on undifferentiated Kennedy Group.|Limestone, dense to microcrystalline and locally calcarenite.|07-FEB-19
28210|Colalura Sandstone|23279|6|Mentioned|p28|||(Playford et al., 1976).||||||
28210|Colalura Sandstone|23816|4|Described|p243, 244|Bajocian|Bajocian|Geological Province: Perth Basin. Of the Champions Bay Group. Underlying unit: Moonyoonooka Sandstone (disconformable). Overlying units: Bringo Shale and Newmarracarra Limestone (conformable). Max. thickness: 8.5 m.||||||27-APR-05
28210|Colalura Sandstone|24020|5|Briefly described|p387|||Shallow marine deposit. Geological Province: Perth Basin||||||16-MAR-05
28210|Colalura Sandstone|30948|6|Mentioned|Map legend|Bajocian|Bajocian|||||||
28210|Colalura Sandstone|31396|6|Mentioned|p1183|||See also P1184.||||||
28210|Colalura Sandstone|31561|6|Mentioned|p22|||Section||||||
28210|Colalura Sandstone|31706|6|Mentioned|p665|||Jurassic correlation chart||||||
28210|Colalura Sandstone|31910|6|Mentioned|p22|||||||||
28210|Colalura Sandstone|32648|6|Mentioned|p32|||Champion Bay Gp.||||||
28210|Colalura Sandstone|32649|4|Described|p24|||Table 1||||||
28210|Colalura Sandstone|33022|6|Mentioned|p259|||||||||
28210|Colalura Sandstone|33166|6|Mentioned|p63|||Refers Arkell & Playford (1954)||||||
28210|Colalura Sandstone|34721|6|Mentioned|p286|||||||||
28210|Colalura Sandstone|35282|6|Mentioned|Fig.27|||||||||
28210|Colalura Sandstone|36257|6|Mentioned|Table 2.1|||||||||
28210|Colalura Sandstone|36293|2|Defined|p147|Bajocian|Bajocian|||||||
28210|Colalura Sandstone|36890|3|Fully described|p243|||||||||
28210|Colalura Sandstone|38444|6|Mentioned|p300|||||||||
28210|Colalura Sandstone|41284|4|Described|p91|||||||||
28210|Colalura Sandstone|43495|6|Mentioned|16|||||||||
28210|Colalura Sandstone|44144|4|Described|p506 Tb.4-21|Aalenian|Aalenian|Type Section: Spion Kop 28o46'44S 114o48'24''E. 8m thick shallow marine sediments containing molluscs and wood.||Champion Bay Group||Disconformably overlies Moonyoonooka Sandstone. Overlain by Bringo Shale (conformably) and Newmarracarra Limestone (disconformably).|Yellow-brown coarse-grained sandstone, commonly conglomeratic, with claystone, siltstone and shale intercalations.|
28210|Colalura Sandstone|61811|4|Described|pp29-31, p34, p63.|Middle Jurassic|Middle Jurassic|A thin unit containing phosphate nodules, fossil wood, leached shell debris and rare plesiosaur remains. Type section is on Spion Kop, a prominent breakaway near Moonyoonooka property; further details in Appendix 1.||Basal unit in Champion Bay Group.||Unconformably overlies Moonyoonooka Sandstone. Is overlain by Bringo Shale.|Friable, ferruginous, conglomeratic sandstone; originally a shelly limestone before weathering.|
28210|Colalura Sandstone|64635|5|Briefly described|p16|Middle Jurassic|Middle Jurassic|||Of the Champion Bay Group.||||
28210|Colalura Sandstone|68135|6|Mentioned|p64|||||||||
28210|Colalura Sandstone|73153|6|Mentioned|p284|Bajocian|Bajocian|Holotype material[?] (UWA 82469) for Ozraptor subotaii (an indeterminate theropod) was recovered from this unit in Western Australia.||||||
34907|Collier Group|22896|6|Mentioned|103|||Geol. province: Bangemall Basin.||||||18-JAN-07
34907|Collier Group|22905|4|Described|p53 Table 1|Mesoproterozoic|Mesoproterozoic|Supersedes Mucalana (Muhling and Brakel, 1985) and Collier (Cooper et al, 1998a) Subgroups. Unconformably overlies the Edmund Group.||||||28-JUL-08
34907|Collier Group|23485|4|Described|p30|Paleoproterozoic|Paleoproterozoic|Formerly Collier Subgroup. Of Bangemall Supergroup. Geological Province: Collier Basin.||||||07-NOV-08
34907|Collier Group|23525|5|Briefly described|p28|||Of the Bangemall Supergroup.  Geological Province: Collier Basin.||||||28-JUL-08
34907|Collier Group|23529|5|Briefly described|p6|||Of the Bangemall Supergroup.  Geological Province: Bangemall Superbasin.||||||28-JUL-08
34907|Collier Group|24017|4|Described|p21|Mesoproterozoic|Mesoproterozoic|Formerly the Collier Subgroup. Of the Bangemall Supergroup. Geological Province: Collier Basin.||||||28-JUL-08
34907|Collier Group|24115|4|Described|p2, p28|Mesoproterozoic|Mesoproterozoic|Of the Bangemall Supergroup. Age: >1070 Ma. Overlies the Edmund Group. Geological Province: Collier Basin.||||||
34907|Collier Group|24161|5|Briefly described|p7|Mesoproterozoic|Mesoproterozoic|Unconformably overlain by the Sunbeam Group. Geological Province: Collier Basin.||||||
34907|Collier Group|24183|2|Defined|p1, p20|Stenian|Ectasian|Max. Thickness: 6400m. Unconformably overlies the Fortescue, Hamersley, Bryah and Earaheedy Groups. Overlain by the Salvation Group. Age: c.1211-1070 Ma.||||||
34907|Collier Group|24522|6|Mentioned|p80 Fig. 2|||Geological Province: Bangemall Basin (WA)||||||
34907|Collier Group|24535|4|Described|p2|Mesoproterozoic|Mesoproterozoic|Thickness: 3 km. Deposited before 1070 Ma (younger dolerite sills intruding). Unconformably underlain by the Scorpion Group. Of the Bangemall Supergroup. Geological Province: Collier Basin.||||Overlies Edmund Group. Unconformably overlies Scorpion Group.||26-NOV-13
34907|Collier Group|24544|4|Described|p43|Mesoproterozoic|Mesoproterozoic|Deltaic to deep marine siliciclastic facies. Of Bangemall Supergroup.||||||26-FEB-13
34907|Collier Group|24578|4|Described|p776 Fig.1, p778 Fig.3|Mesoproterozoic|Mesoproterozoic|Of the Bangemall Supergroup. Age: ~1200 Ma. Geological Province: Collier Basin.||||||
34907|Collier Group|50008|5|Briefly described|p47 Fig.4|Mesoproterozoic|Mesoproterozoic|Of Bangemall Supergroup.||||||
34907|Collier Group|50010|5|Briefly described|p53, 54|Mesoproterozoic|Mesoproterozoic|Age: c. 1070 Ma. Unconformably overlies Edmund Group. Correlates with Manganese Group. Of Bangemall Supergroup.||||||18-JAN-07
34907|Collier Group|50188|5|Briefly described|p2 Fig. 1, p12 Tb. 1|||Of the Bangemall Supergoup.  Geological Province: Bangemall Basin.||||||16-JUL-08
34907|Collier Group|50222|5|Briefly described|p319 Fig. 2, p334 Tb.2|Mesoproterozoic|Mesoproterozoic|Age: 1.20-1.10Ga.   Geological Province: Collier Basin.||||||
34907|Collier Group|50225|4|Described|p386 Fig. 1, p395|||Of Bangemall Supergroup. Comprises Backdoor, Calyie and Ilgarari Formations. Unconformably overlies Coodardoo Fm, + in the south overlies Ullawarra Fm + Curran Member. Age: c.1400-1070Ma.  Geol Prov: Edmund Basin. See also p407.||||||07-FEB-11
34907|Collier Group|50226|5|Briefly described|p424 Fig. 5, p426|||Of the Bangemall Supergroup.  Mainly siltstone beds.  Unconformably overlies Edmund Group.  Geological Province: Bangemall Basin.  See also p427 Fig. 6.||||||
34907|Collier Group|50292|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Bangemall Supergroup.  Geological Province: Collier Basin.||||||31-MAY-04
34907|Collier Group|50334|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Bangemall Supergroup. Geological Province: Bangemall Superbasin.||||||
34907|Collier Group|50380|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Bangemall Supergroup. Geological Province: Collier Basin.||||||07-NOV-08
34907|Collier Group|60301|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Bangemall Supergroup. Geological Province: Collier Basin.||||||
34907|Collier Group|60535|5|Briefly described|p556|Mesoproterozoic|Mesoproterozoic|Age: ca. 1070 Ma. Of the Bangemall Supergroup.||||||
34907|Collier Group|61262|6|Mentioned|p454|||Together with Edmund Group, overlies the Gascoyne Complex.||||||
34907|Collier Group|61564|5|Briefly described|p590 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: ?1.2Ga. Geological Province: Edmund and Collier Basins.||||||
34907|Collier Group|61850|5|Briefly described|p324 Fig. 1||Proterozoic|Of the Bangemall Supergroup. Siltstone, mudstone, sandstone, conglomerate, dolomite and subordinate chert.||||||
34907|Collier Group|63246|5|Briefly described|p478 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Bangemall Supergroup.||||||
34907|Collier Group|63471|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Bangemall Supergroup. Includes Backdoor Formation. Geological Province: Collier Basin.||||||12-SEP-07
34907|Collier Group|63866|4|Described|p152-p153, p162-p163, p168, p176|Ectasian|Calymmian|Edmund/Collier Basins. Between 2 to 2.5km thick. The minimum age for this group is constrained on the basis of intruding dolerite sills in the Backdoor and Ilgarari Formations.|c. 1400 Ma (inferred, constituent)||Includes the Backdoor, Calyie and Ilgarari Formations.|Unconformably overlies the Bryah, Padbury, Eraheedy, Fortescue and Hamersley Groups. Disconformably overlies the Edmund Group.|Siliciclastic sedimentary rock.|
34907|Collier Group|63869|4|Described|p1, p4, p5, p27-28, p31, p37, p39-43|Mesoproterozoic|Mesoproterozoic|See also p47, p51, Plate 1. Martin et al. (1999); Martin and Thorne, (2002); formerly Collier Subgroup (of Bangemall Group). Collier Basin. Thickness c.2.5 km. Correlated with (now obsolete) Mucalana Subgroup of Muhling and Brakel (1985). Mainly siliciclastic sedimentary rocks. Intruded by one suite of dolerite sills aged 1070 Ma. Maximum age from detrital zircons (Cawood and Nemchin, 2002). Minimum age from dolerite sills (Wingate, 2002).|c.1400-c.1070 Ma.|Unit in Bangemall Supergroup.|Includes Backdoor, Calyie and Ilgarari Formations.|Unconformably overlies Gascoyne Complex, and Wyloo, Edmund, Fortescue, Hamersley, Bryah and Earaheedy Groups. Disconformably overlies Edmund Group.|Dominantly siltstone, fine- to very coarse-grained sandstone, pebbly sandstone, dolostone and minor chert and conglomerate. Intruded by thick dolerite and gabbro sills.|
34907|Collier Group|64283|5|Briefly described|p49, p50 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Bangemall Supergroup. Probably correlates with Oldham Sandstone; also with the Manganese Group in the north. .||||||07-FEB-11
34907|Collier Group|64284|5|Briefly described|p58 Fig. 1, p62 Fig. 3|||Of the Bangemall Supergroup. Geological Province: Bangemall Basin.||||||07-FEB-11
34907|Collier Group|64285|5|Briefly described|p67 Fig. 2|||Of the Bangemall Supergroup. Geological province: Bangemall Basin.||||||07-FEB-11
34907|Collier Group|64286|6|Mentioned|p74|Mesoproterozoic|Mesoproterozoic|Age: c.1.2Ga. See also Table 1.||||||07-FEB-11
34907|Collier Group|64287|5|Briefly described|p31|||Uppermost in the Bangemall Supergroup. Unconformably overlies by Edmund Group. Geological Province: Jillawarra Sub-basin.||||||07-FEB-11
34907|Collier Group|64580|4|Described|map legend||Mesoproterozoic|Siltstone, mudstone, sandstone; minor dolostone, chert, and conglomerate. Includes BACKDOOR FORMATION and CALYIE FORMATION; siltstone, mudstone, and fine-grained sandstone. Includes ILGARARIE FORMATION.||||||14-NOV-11
34907|Collier Group|64722|5|Briefly described|p7|Stenian||Of Mesoproterozoic Collier Basin. Sediment sourced from Edmund Group plus input from Pilbara Craton and Paterson Orogen.||Upper unit of Bangemall Supergroup.||Unconformably overlies Edmund Group.||11-APR-12
34907|Collier Group|64724|5|Briefly described|p48, p49 Fig. 7|Stenian|Stenian|Deposited in the Collier Basin during the Musgrave event during the early Stenian.||||||
34907|Collier Group|64728|5|Briefly described|pp93-95, p108.|Mesoproterozoic|Mesoproterozoic|Collier Basin. Records unroofing and reworking of Edmund Group, with possible additional material from Pilbara Craton and Paterson Orogen. Intruded by dolerite sills aged c.1070 Ma.||Upper unit in Bangemall Supergroup.|Includes Calyie, Backdoor and Ilgarari  Formations.|Is unconformably underlain by Edmund Group.||15-SEP-14
34907|Collier Group|64772|5|Briefly described|p13, Plate 1, p14, 20-21, 25|Mesoproterozoic|Mesoproterozoic|Superseded Collier Subgroup. Comprises Backdoor and Calyie Formations. Unconformably overlies Earaheedy and Scorpion Groups. Age: between 1210 and 1070Ma. Geological province: Collier Basin. Some of its rocks now assigned to Scorpion Group.||||Probable correlative of the Salvation Group (Hocking et al. 2003);||25-NOV-13
34907|Collier Group|64777|5|Briefly described|p6-7 |Mesoproterozoic|Mesoproterozoic|Intruded by dolerite sills with SHRIMP U-Pb zircon and baddeleyite ages of 1465 and 1070 Ma (Wingate 2002). Includes detrital zircons of 1780 Ma (Nelson 2002).|>1465 Ma|Of the Bangemall Supergroup||||
34907|Collier Group|64872|6|Mentioned|p24 Fig.1|Mesoproterozoic|Mesoproterozoic|Unit in Bangemall Supergroup. ||||||
34907|Collier Group|65152|5|Briefly described|p2 Fig.1, p3.|Mesoproterozoic|Mesoproterozoic|Unit in Bangemall Supergroup. Fine-grained siliciclastics and carbonates. Folding and low-grade metamorphism caused by Edmundian Orogeny.||||||01-MAY-15
34907|Collier Group|65450|5|Briefly described|p2 Fig.1, p3|Mesoproterozoic|Mesoproterozoic|Dolerite sill intrusion dated at around 1070 Ma.||||||05-JAN-17
34907|Collier Group|65472|6|Mentioned|p5 Fig. 4|||Collier Basin.||Bangemall Supergroup||||
34907|Collier Group|65506|4|Described|p986-988, p990-994, p996-997, p999||<1352 +/- 89 Ma.|2300m thick, siliciclastic rocks. Unconformably overlies Edmund Group. U-Pb detrital zircon maximum depositional age (Cawood and Nemchin, (pers.comm.). Narimbunna Dolerite in betweeen Collier Group and Edmund Group. Part of Bangemall Supergroup.||||||
34907|Collier Group|65829|6|Mentioned|p27.|||||||||
34907|Collier Group|65830|5|Briefly described|p1, p4, p8, p9, p11, p13, p16-19, p25-26|Stenian|Statherian|See also Plate 1. Collier Subgroup was elevated to the Collier Group by Martin et al. (1999) during a revision of the former Bangemall Group. ~ 2-2.5 km thick. Maximum age from detrital zircons in Backdoor Formation; minimum age from dolerite sills, which intruded wet sediment, suggesting true age is close to this minimum.|Between c.1620 Ma and c.1070 Ma.|Of the Bangemall Supergroup|Includes Backdoor Formation, Calyie Formation, Ilgarari Formation.|Unconformably underlain by the Edmund Group.||
34907|Collier Group|65896|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Collier Basin. Upper part of Bangemall Supergroup, from 1211 to 1070 Ma. Includes Wonyulgunna Sandstone, Backdoor and Calyie Formations.||||||
34907|Collier Group|66104|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Collier Basin. Upper part of Bangemall Supergroup; age shown as  >1070 Ma. Includes  Backdoor, Calyie and Ilgarari Formations.||||||
34907|Collier Group|66107|5|Briefly described|p1, p4, p5 |Mesoproterozoic|Mesoproterozoic|Minimum age constrained by dolerite sills.|ca.1070 Ma minimum.||Includes the Ilgarari Formation, Calyie Formation and Backdoor Formation.|Unconformably overlies the Edmund Group. Possibly correlative of Manganese and Kahrban Groups, and the Cornelia Sandstone.|Shale, sandstone, dolomite.|
34907|Collier Group|66112|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Collier Basin. Unit in Bangemall Supergroup. Comprises Backdoor and Calyie Formations. Intruded by dolerite and gabbro sills of the Kulkatharra Dolerite.||||||
34907|Collier Group|66241|4|Described|pp1-4, p9, pp28-29. |Mesoproterozoic|Mesoproterozoic|Collier Basin. Sediments were wet when intruded by Kulkatharra Dolomite, hence depositional age is close to 1070 Ma.|<1465 Ma to >1070 Ma.|Unit in Bangemall Supergroup.|Includes Backdoor, Calyie and Ilgarari Formations.|Disconformably overlies Edmund Group.|Fine- to medium-grained siliciclastic rocks.|
34907|Collier Group|66299|6|Mentioned|p4 Fig.2, p333.|Mesoproterozoic|Mesoproterozoic|Intruded by sills of Kulkatharra Dolerite and Mundine Well Dolerite Suite. ||||||
34907|Collier Group|66427|6|Mentioned|p41 Tb.1, p43 Fig.2|||Intruded by mafic sills and dykes 1.07 Ga.|1.2 - 1.07 Ga.|||||
34907|Collier Group|66887|5|Briefly described|p5 Fig.4|Mesoproterozoic|Mesoproterozoic|Gascoyne Province.|~1450-~1070 Ma estimated from Fig.4.|||||
34907|Collier Group|66950|6|Mentioned|p9 Fig.8, p12, p13|Stenian|Calymmian||c. 1500-1000 Ma|||||
34907|Collier Group|67136|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin.||Unit in Bangemall Supergroup.|Includes Backdoor, Calyie and Ilgarari Formations.|Is intruded by Kulkatharra Dolerite sills.||
34907|Collier Group|67245|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin.||Unit in Bangemall Supersuite.|Includes Backdoor Formation.|||
34907|Collier Group|67269|5|Briefly described|p20-21 Fig.19|Stenian|Calymmian|Bangemall Basin.|1465-1070 Ma.||Stag Arrow Formation.|||
34907|Collier Group|67346|6|Mentioned|p794 Fig.1|Mesoproterozoic|Mesoproterozoic|Edmund and Collier Basins.||||||11-MAY-12
34907|Collier Group|67374|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin.||Unit in Bangemall Supergroup.|Includes Backdoor, Calyie and Ilgarari Formations.|Intruded by sills of Kulkatharra Dolerite.||
34907|Collier Group|67888|6|Mentioned|p54|Mesoproterozoic|Mesoproterozoic||1465-1070 Ma|Bangemall Supergroup||Overlies Edmund Group||
34907|Collier Group|68055|6|Mentioned|p76-77|||Bangemall Superbasin.||Bangemall Supergroup.||||
34907|Collier Group|68280|6|Mentioned|p26 fig 24|||Bangemall Basin.|~1300 - 1000 Ma||Includes Stag Arrow Formation|||24-MAY-19
34907|Collier Group|68285|5|Briefly described|Map Legend|Stenian|Calymmian|Collier Basin. Age constrained by age of younger Kulkatharra Dolerite (c. 1070 Ma) and older Narimbunna Dolerite (c. 1465 Ma)|c. 1465-1070 Ma|Of the Bangemall Supergroup.|Includes Ilgarari Formation, Calyie Formation, Backdoor Formation.|Intruded by the Kulkatharra Dolerite.||
34907|Collier Group|68286|5|Briefly described|Map Legend|Stenian|Calymmian|Collier Basin. Age constrained by age of younger Kulkatharra Dolerite (c. 1070 Ma) and older Narimbunna Dolerite (c. 1465 Ma)|c. 1465-1070 Ma|Of the Bangemall Supergroup.|Includes Ilgarari Formation, Calyie Formation, Backdoor Formation.|Intruded by the Kulkatharra Dolerite.||
34907|Collier Group|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic|||Bangemall Supergroup|Includes Backdoor Formation, Calyie Formation.|||
34907|Collier Group|69003|4|Described|p4, p9 Fig.9, p34, p53, p56|Mesoproterozoic|Mesoproterozoic|Collier Basin, Capricorn Orogen. c.2000m thick. Age weakly constrained: unaffected by 1385-1200 Ma Mutherbuckin Tectonic Event, and formation of peperite in the lower parts indicates wet sediments deposited shortly before intrusion, ie c.1070 Ma. Underwent folding and faulting during the 1030-955 Ma Edmundian Orogeny.|||Backdoor, Calyie and Ilgarari Formations.|Unconformably overlies Edmund Group. Is intruded by Kulkatharra Dolerite.|Succession of shallow-marine to shelfal siliciclastic sedimentary rocks; includes interbedded siltstones and sandstones.|
34907|Collier Group|69010|5|Briefly described|Map Legend|Stenian|Calymmian|Collier Basin.|1460-1070 Ma|Of the Bangemall Supergroup.|Includes Ilgarari Formation, Calyie Formation, and Backdoor Formation.|Intruded by Kulkatharra Dolerite.||24-APR-14
34907|Collier Group|69027|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Collier Basin. Intruded by dolerite and gabbro sills at around c. 1070 Ma (Wingate, 2002; Nelson 2004). See map legend for a detailed lithological description.|||Includes Ilgarari Formation, Calyie Formation, and Backdoor Formation.|Underlain by the Edmund Group.|Includes siltstone, mudstone, sandstone, conglomerate, dolostone, minor chert, dololutite, dolomitic siltstone, and dolarenite.|
34907|Collier Group|69028|5|Briefly described|Map Legend|Stenian|Stenian|Collier Basin.|1200-1075 Ma.||Includes Ilgarari, Backdoor and Calyie Formations.|Intruded by the Kulkatharra Dolerite.|Siltstone, mudstone, sandstone, dolostone, chert and conglomerate.|06-MAY-14
34907|Collier Group|69080|5|Briefly described|p684, p690-692, p694, p697|Stenian|Stenian|Gascoyne Province. Deposition occurred between faulting at c.1200 Ma and intrusions at c.1070 Ma. Detritus was sourced primarily from underlying Edmund Group.||||Intruded by Kulkatharra Dolerite sills.|Siltstone, mudstone, sandstone; minor dolostone, chert and conglomerate.|
34907|Collier Group|69091|5|Briefly described|p180|||Regional outcrop trends in eastern Capricorn Orogen suggest Salvation Group overlies, and may interfinger with, upper Collier Group, rather than being equivalent, as suggested by Grey et al. (2005), and thus probably forms part of Collier Basin. ||||||
34907|Collier Group|69166|4|Described|geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic||||Includes Backdoor Formation, Jeeaila Sandstone Member, Calyie Formation, Ilgarari Formation||Siltstone, mudstone, sandstone; minor dolostone, chert, and conglomerate.|
34907|Collier Group|69185|5|Briefly described|500k_geologyp08_lut.csv||Mesoproterozoic|||Unit of Bangemall Supergroup.|Includes Backdoor Formation, Calyie Formation, Ilgarari Formation.||Siltstone, mudstone, and fine-grained sandstone.|
34907|Collier Group|69237|6|Mentioned|p2|Mesoproterozoic|Mesoproterozoic|||Bangemall Supergroup.||||
34907|Collier Group|69546|6|Mentioned|p102|Mesoproterozoic|Mesoproterozoic|Geological province: Gascoyne Province.||||||
34907|Collier Group|69596|5|Briefly described|p4-8, p12-13|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen. Deposition occurred after the 1385-1170 Ma Mutherbukin Tectonic Event. Detritus sourced mainly from Edmund Basin. Underwent widespread folding and low-grade metamorphism during the 1030-955 Ma Edmundian Orogeny. Hosts several major copper and base metal deposits.||Bangemall Supergroup.|Backdoor, Calyie, Ilgarari Formations.|Is intruded by Kulkatharra Dolerite.||
34907|Collier Group|70019|6|Mentioned|p93-94|Proterozoic|Proterozoic|Geological province: Gascoyne Province, Capricorn Orogen.||||Underlain by Coodardoo Formation/Edmund Group.||
34907|Collier Group|70132|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Coller Basin. Deposited after the Mutherbukin Tectonic Event (1321-1171 Ma).|<1171 - 1084 Ma.|Bangemall Supergroup.|Backdoor, Calyie and Ilgarari Formations.|Is intruded by Kulkatharra Dolerite.|Siltstone, sandstone, chert, dolostone, conglomerate.|
34907|Collier Group|70136|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Collier Basin.|c.1170-c.1070 Ma.|Bangemall Supergroup.|Backdoor, Calyie and Ilgarari Formations.|Is intruded by Kulkatharra Dolerite.||
34907|Collier Group|70767|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin.||Bangemall Supergroup.|Backdoor, Calyie, Ilgarari Formations.|Overlies Edmund Group. Is intruded by Kulkatharra Dolerite.||
34907|Collier Group|70768|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin.||Bangemall Supergroup.|Backdoor, Calyie, Ilgarari Formations.|Overlies Edmund Group. Is intruded by Kulkatharra Dolerite.||
34907|Collier Group|70795|5|Briefly described|100k_geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Also 2_5m_interpgeop15_lut.csv, West Australian Craton|1171-1070 Ma|Bangemall Supergroup|Includes Ilgarari Formation, Calyie Formation, Backdoor Formation|Intruded by Kulkatharra Dolerite, Unconformably overlies Ullawarra Formation|Undivided siliciclastic rock; minor dolostone and chert.|
34907|Collier Group|70796|4|Described|2_5m_interpgeop15_lut.csv|Mesoproterozoic|Mesoproterozoic|Of the Collier Basin, Capricorn Orogen. Affected by the Edmundian Orogen (1026954 Ma). See also 500k_interpgeop14_lut.csv.|ca. 1171 1070 ma (inferred)|Bangemall Supergroup|||Siltstone, mudstone, sandstone; minor dolostone, chert, and conglomerate.|
34907|Collier Group|70814|5|Briefly described|iii, iv, p2-p4, p5, p15, p17, p19, |Mesoproterozoic|Mesoproterozoic|Collier Basin. Note ages are poorly constrained and as such the ages provided are considered to be tentative. Deposition, provenance and tectonic setting are discussed in detail. See also p21-p23, p25-p30, p32, p36-p39, p41, p48-p49, p57.|ca 1171-1069 Ma||Includes the Backdoor, Calyie and Ilgarari Formations.|Intruded by the Kulkatharra Dolerite.||
34907|Collier Group|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Collier Basin.Capricorn Orogen.||Bangemall Supergroup||||
34907|Collier Group|70936|5|Briefly described|p58-p59,61,74|Stenian|Stenian|Geological province: Pilbara Craton. Of Collier Basin. Correlable with Manganese Group. Widespread intrusion of dolerite sills at c. 1070 Ma. Some dolerites have pepperitic margins, indicating intrusion into wet/unconsolidated sediments, with SHRIMP U-Pb zircon age of 1076+\-4 Ma. Deposition also post-dates Motherbukin event which ceased at c. 1200 Ma. Therefore, Collier Group deposition constrained between 1200 and 1070 Ma.|>1070 Ma|Unit of Bangemall Supergroup.||||16-AUG-19
34907|Collier Group|70949|6|Mentioned|p988|Mesoproterozoic|Mesoproterozoic|||||||
34907|Collier Group|71003|5|Briefly described|p58-p59, p61, p74|Stenian|Stenian|Pilbara Craton.Interpreted as part of the newly named Wongawobbin Basin. Also referred to as the Collier Subgroup on p74. The minimum age is derived from dating of dolerite sills intersecting this unit.|c.1465-1070 Ma|Bangemall Supergroup|Includes the Backdoor Formation.|Partially correlated with the Manganese Group. Unconformably overlies the Edmund Group.||
34907|Collier Group|71042|6|Mentioned|p66 fig 2, p67|Mesoproterozoic|Mesoproterozoic|Southern Pilbara.||Of Bangemall Supergroup.||||24-MAY-19
34907|Collier Group|71158|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin.||Bangemall Supergroup.|Backdoor, Calyie, Ilgarari Formations.|Is intruded by  Kulkatharra Dolerite.||
34907|Collier Group|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Bangemall Supergroup.|Includes Calyie Formation.||shale, siltstone, claystone, sandstone|
34907|Collier Group|71269|5|Briefly described|GEOL_LUT_CSV files|||Geological province: Capricorn Orogen; West Australian Craton. See 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv.||Unit of Bangemall Supergroup.|Includes Backdoor Formation, Calyie Formation.|Intruded by Kulkatharra Dolerite.|Undivided siliciclastic rock; minor dolostone and chert|
34907|Collier Group|71484|5|Briefly described|p125|||Geological province: Of Edmund and Collier basins. Intruded by Kulkatharra Dolerite.||Unit of Bangemall Supergroup.|||Silstone, mudstone, sandstone; dolostone, chert and conglomerate.|30-AUG-19
34907|Collier Group|71804|5|Briefly described|p392, p403 fig 10|||Gascoyne Province. Geochronology results, interpretation and methodology are discussed.|ca. 1170-1070 Ma|||||
34907|Collier Group|71869|6|Mentioned|p3-p4|||Capricorn Orogen.|1171-1071 Ma|Bangemall Supergroup||||
34907|Collier Group|72259|6|Mentioned|p3|Stenian|Stenian||ca. 1200-1075 Ma||Ilgarari Formation, Backdoor Formation, Calyie Formation|||
34907|Collier Group|72705|5|Briefly described|p3-4|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.|||Backdoor, Calyie, Ilgarari Formations.|Overlies Edmund Group.||
34907|Collier Group|73102|5|Briefly described|p1, p3|||Gascoyne Province. Hosts extensive dolerite sills of the Narimbunna Dolerite and Kulkatharra Dolerite.||||Intruded by Kulkatharra Dolerite.|Siltstone, mudstone, sandstone; minor dolostone, chert, and conglomerate.|
34907|Collier Group|73214|5|Briefly described|p974 Fig.1|Mesoproterozoic|Mesoproterozoic|Mapped in Fig. 1 as one unit with Edmund Group. Affected by the 1320-1170 Ma Mutherbukin Event and the 1030-900 Ma Edmundian Orogeny.||||||
34907|Collier Group|73442|5|Briefly described|p1, p3, p20|Proterozoic|Proterozoic|Capricorn Orogen. Unconformably overlies Gascoyne Province and the margins of Archean cratons. Intruded by mafic sills.|||Ilgarari Formation|Intruded by Kulkatharra Dolerite|Low-grade, variably deformed metasedimentary rocks comprising siltstone, mudstone, sandstone; minor dolostone, chert and conglomerate.|
35659|Colonial Chert Member|23126|5|Briefly described|p383 Fig.3|||||||||
35659|Colonial Chert Member|23612|5|Briefly described|p843|||||||||
35659|Colonial Chert Member|24426|5|Briefly described|p220|Paleoproterozoic|Archean|Top of Mount McRae Shale. Thickness: ~10-15m. Geological Province: Hamersley Province. Enriched in banded iron-formation.||||||07-FEB-11
35659|Colonial Chert Member|67056|6|Mentioned|p419 Fig.2. |||||Unit in Mount McRae Shale.||Is overlain by Dales Gorge Member of Brockman Iron Formation.||
35659|Colonial Chert Member|71513|6|Mentioned|p67, p70, p74, p85, p88|||Intersected in drillholes DDH44 and Mitchell-2.||Mt McRae Shale||||
35659|Colonial Chert Member|71808|5|Briefly described|p27-p28, p30, p133|||Hamersley Province.||Dales Gorge Member||Overlain by the Dales Gorge Member.|Chert and biffy chert with shale interbeds.|
35659|Colonial Chert Member|73022|5|Briefly described|p3, p6, p7 Fig.9|||Some ferruginous chert beds contain greenalite nanoparticles, syneresis structures and shrinkage structures indicting a depositional origin from hydrothermal vent plumes.||Mount McRae Shale||Underlies the Brockman Iron Formation, Dales Gorge Member.|Laminated chert intercalated with fine-grained marine carbonate and siliciclastic siltstone and shale. Ferruginous chert interval with minor shale, banded iron formation.|
23498|Comet Vale Monzogranite|42221|5|Briefly described|p34|||||||||
23498|Comet Vale Monzogranite|42382|4|Described|p38|||See also Fig.6 P40||||||
23498|Comet Vale Monzogranite|42696|6|Mentioned|Plate 1B|Archean||||||||07-NOV-08
23498|Comet Vale Monzogranite|42742|5|Briefly described|map legend|Archean||||||||07-NOV-08
23498|Comet Vale Monzogranite|43074|5|Briefly described|p17,p30|||see also Fig.6.||||||
23498|Comet Vale Monzogranite|50075|5|Briefly described|p16|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
23498|Comet Vale Monzogranite|50076|5|Briefly described|Map|Archean|Archean| Porphyritic biotite monzogranite.  Geological Province: Yilgarn Craton.||||||07-NOV-08
23498|Comet Vale Monzogranite|60076|5|Briefly described|p45 App. 1|||[Agmcv]   Fine- to medium-grained, porphyritic monzogranite.||||||
23498|Comet Vale Monzogranite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Fine- to medium-grained, porphyritic monzogranite; local foliation; discordant contact with greenstones.||||||07-FEB-11
23498|Comet Vale Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Fine to medium grained, porphyritic monzogranite; local foliation; discordant contacts with greenstones.|05-AUG-15
23498|Comet Vale Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Fine to medium grained, porphyritic monzogranite; local foliation; discordant contacts with greenstones.|
23498|Comet Vale Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
23498|Comet Vale Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv, 100k_geologysub10_lut.csv.|2692-2600 Ma (inferred)||||Porphyritic monzogranite, fine to medium grained; metamorphosed|
35911|Comstock Member|23348|5|Briefly described|217|||||||||
35911|Comstock Member|23784|5|Briefly described|p24|||Supersedes Comstock Andesite.  Of Rushall Slate.||||||
35911|Comstock Member|23793|5|Briefly described|p24|Archean|Archean|Formerly Comstock Andesite Member. Of Rushall Slate.||||||15-DEC-08
35911|Comstock Member|24185|5|Briefly described|p746 Tb.4|||Parent: Rushall Slate.||||||
35911|Comstock Member|64174|5|Briefly described|Map legend|Archean|Archean|Of the Bookingarra Formation (Croydon Group, De Grey Supergroup).  Geological province: Mallina Basin. Fine-grained intrusive rock; vesicular with rare pyroxene spinifex-texture; metamorphosed.||||||07-NOV-08
35911|Comstock Member|64580|4|Described|map legend||Mesoarchean|Of Bookingarra Formation. Fine grained intrusive rock; vesicular, with rare pyroxene spinifex-texture; metamorphosed.||||||15-DEC-08
35911|Comstock Member|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Bookingarra Formation.|||Fine grained intrusive rock; vesicular, with rare pyroxene spinifex-texture; metamorphosed|
35911|Comstock Member|69299|5|Briefly described|p6 Tb.1|Archean|Archean|||Of Rushall Slate.|||High-Mg and vesicular basalt.|
35911|Comstock Member|69300|5|Briefly described|map legend|Archean|Archean|Mallina Basin, Whim Creek greenstone belt.||Mount Negri Volcanics|||Vesicular metabasalt; sub-volcanic intrusive; metamorphosed|02-SEP-14
35911|Comstock Member|70775|5|Briefly described|p24 tbl 3, p29 tbl 5, p55, p60, p76|Mesoarchean|Mesoarchean|Previously known as the Comstock Andesite Member of Miller and Gair (1975). Up to 100m thick.|c. 2955 Ma (Smithies et al, 2007a)|Rushall Slate|||Basalt.|
23500|Condenser Dolerite|22534|6|Mentioned|Fig.5 p10|||Of Black Flag Group.||||||14-APR-08
23500|Condenser Dolerite|23137|4|Described|p245 Table.2|||||||||
23500|Condenser Dolerite|23795|6|Mentioned|p12|||Geological Province: Yilgarn Craton.||||||
23500|Condenser Dolerite|23926|6|Mentioned|p16 Fig. 5|||||||||
23500|Condenser Dolerite|41066|6|Mentioned|2 of 2 J03|||||||||
23500|Condenser Dolerite|41588|6|Mentioned|Table 1|||||||||
23500|Condenser Dolerite|41784|6|Mentioned|Table 1|||||||||
23500|Condenser Dolerite|42117|5|Briefly described|Table 1 P67|||||||||
23500|Condenser Dolerite|42221|6|Mentioned|Table 1 P6|||||||||
23500|Condenser Dolerite|42696|6|Mentioned|Plate 1B|||||||||
23500|Condenser Dolerite|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
23500|Condenser Dolerite|43102|5|Briefly described|Fig.3|||||||||
23500|Condenser Dolerite|43162|6|Mentioned|5|||||||||
23500|Condenser Dolerite|43496|6|Mentioned|15|||Age: 2762+/-32Ma.||||||14-APR-08
23500|Condenser Dolerite|60514|6|Mentioned|p25 Fig. 2, p27 Fig. 4, p43|Archean|Archean|Intrudes Black Flag Group. Age: 2680+/-8 Ma, (Carey, 1994). Max thickness: 500m. Sub-vertical sill, and intrudes along the contact between the Paringa Basalt and Black Flag Group. Geol Prov: Yilgarn Craton.||||||07-FEB-11
23500|Condenser Dolerite|60623|4|Described|p25 Fig.2, p43|Archean|Archean|Thickness: up to 500m. Intrudes contact between Paringa Basalt and Black Flag Group. Geochemically different from other lavas in the area. Lateral equivalents of Golden Mile Dolerite. Divided into 4 internal zones. Geological Province: Eastern Goldfields.||||||07-NOV-08
23500|Condenser Dolerite|60627|5|Briefly described|p65 Tb.1|||Intrudes Black Flag Group.||||||14-APR-08
23500|Condenser Dolerite|62108|5|Briefly described|p1409 Tb. 13|||Geological Province: Yilgarn Craton (Boulder-Lefroy Shear Zone). See also p1417 Fig. 10.||||||07-FEB-11
23500|Condenser Dolerite|62109|5|Briefly described|p1428|Archean|Archean|Sill that intrudes the lower Black Flag Group.Age: 2680+/-8Ma.||||||07-NOV-08
23500|Condenser Dolerite|65834|6|Mentioned|p7|||Kambalda Domain, Kalgoorlie Terrane.||Black Flag Group.||||
23500|Condenser Dolerite|68289|6|Mentioned|p31|||||||||
23500|Condenser Dolerite|69631|6|Mentioned|p28|||||||||
23500|Condenser Dolerite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2680 +/- 8 Ma (isotopic age).|Great Boulder Suite|||Tholeiitic differentiated sill; pyroxene-bearing dolerite to gabbro; quartz-plagioclase granophyric zones in upper sections; minor aphyric basalt at margins; metamoprhosed.|
23500|Condenser Dolerite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).  See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2680+\-8 Ma|Unit of Great Boulder Suite.|||Tholeiitic differentiated sill; pyroxene-bearing dolerite to gabbro; quartz--plagioclase granophyric zones in upper sections; minor aphyric basalt at margins; metamoprhosed|
23500|Condenser Dolerite|72049|5|Briefly described|p258, p272|||St Ives. Age of Carey, 1994. See also Condensor Dolerite p253, 258, 259, 267, 268.|2680+/-8 Ma U-Pb SHRIMP zircon age|||||18-MAR-19
23500|Condenser Dolerite|73391|6|Mentioned|p240, 304, Appendices.|||Kambalda area.|2680 +/- 8 Ma (Carey, 1994).|||||
82172|Connie Sue Formation|73084|4|Described|p: 21, 52, 54-57, 73-77, 80-82, 119, 141|Stenian|Stenian|Nornalup Zone, eastern; Albany-Fraser Orogen. Kepa Kurl Booya Province. Listed age is from a mafic schist. Intruded by weakly deformed, equigranular, pink metamonzogranite dated at 1169 +/- 6 Ma and undeformed, strongly altered, coarse-grained leucogabbro dated at 1180 +/- 8 Ma. Whole-rock geochemical data shows that the mafic volcanic component has similar E-MORB - OIB characteristics to the Pinto Basalt; likely a result of deep asthenospheric upwelling. Report includes lithologic/petrographic description, structural analyses, whole-rock geochemistry.|1172 +/- 7 Ma||||Ca-Mg-rich to Fe-rich metasedimentary rocks, mostly calc-silicate schists, interlayered with metabasalt and/or mafic metavolcaniclastic rocks.|
78533|Connolly Gneiss|70153|5|Briefly described|100k_interpgeop_lut.csv|Mesoarchean|Mesoarchean||2801 +/- 10 Ma (isotopic).||||Biotite-muscovite granitic gneiss; medium grained; schistose.|
78533|Connolly Gneiss|71270|4|Described|100k_interpgeop_lut.csv|Mesoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2801+\-10 Ma||||Biotite-muscovite granitic gneiss; schistose to medium-grained|
69185|Conqueror Porphyry|60623|6|Mentioned|p42 Fig.12|||||||||
38998|Considerable creek pillow basalts|23870|6|Mentioned|p229 Fig.3|||Informal name.||||||
25855|Coobarra Formation|22905|6|Mentioned|p52 Fig. 2|||Of the Edmund Subgroup (Bangemall Group).||||||24-JAN-06
25855|Coobarra Formation|23589|5|Briefly described|p6 Table 2|||1638+/-14 Ma (SHRIMP U-Pb zircon). Of Bangemall Group.||||||
25855|Coobarra Formation|23723|5|Briefly described|p9 Table 1|||Incorporated into the West Creek formation. Geological Province: Bangemall Basin.||||||
25855|Coobarra Formation|23774|6|Mentioned|p733 table 1|||||||||
25855|Coobarra Formation|24183|5|Briefly described|p4 Fig.3, p6|Statherian|Statherian|Of the Edmund Subgroup (Muhling and Brakel, 1985). Age: 1638 +/- 14 Ma||||||
25855|Coobarra Formation|24544|4|Described|p44 Fig.32|Mesoproterozoic|Mesoproterozoic|Of Bangemall Group. Age: 1638+/-14 Ma. Conformably overlain by Irregully Formation.||||||
25855|Coobarra Formation|29916|4|Described|p119|||||||||
25855|Coobarra Formation|36551|6|Mentioned|p101|||||||||
25855|Coobarra Formation|38298|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
25855|Coobarra Formation|38299|4|Described|p8|||||||||
25855|Coobarra Formation|39168|6|Mentioned|p71|||||||||
25855|Coobarra Formation|40088|6|Mentioned|p224|||||||||
25855|Coobarra Formation|40089|2|Defined|p20|Mesoproterozoic|Mesoproterozoic|See also p13.||||||08-MAR-18
25855|Coobarra Formation|40899|6|Mentioned|Fig.1|||||||||
25855|Coobarra Formation|41360|6|Mentioned|Table 1|||||||||
25855|Coobarra Formation|44142|4|Described|p311, p313 Tb.4-4, p318, p321-322|Stenian|Stenian|~500m thick alluvial fan deposits. Limited extent. Within Florry Subgroup of Chuck (1984). Age from rhyolite domes.|1098 +/- 42 Ma (Rb-Sr; Gee et al. 1976)|Edmund Subgroup.||Overlain conformably by Backdoor Formation.|Sandstone, conglomerate; minor siltstone, shale, small plugs (or domes) of rhyolite.|13-MAR-18
25855|Coobarra Formation|50225|5|Briefly described|p387 Fig. 2|||Formerly of the Edmund Subgroup (Bangemall Group) - then reassigned to Tringadee Formation?  And now part of Yilgatherra Formation?||||||07-FEB-11
25855|Coobarra Formation|63866|5|Briefly described|p152, p154, p162, p177|Statherian|Statherian|Ashburton Basin.|1638 +/- 14 Ma (Nelson, 1995)|Edmund Group|Includes the Tangadee rhyolite.|||
25855|Coobarra Formation|63869|5|Briefly described|p28|Calymmian|Statherian|Interpreted maximum age of 1638 +/- 14 Ma based on two zircons in rhyolite.||Unit in Edmund Group.|||Includes rhyolite.|
25855|Coobarra Formation|65408|5|Briefly described|p85 Table2|Statherian|Statherian|Age is of rhyolite emplacement.|1638 +/-14 Ma SHRIMP U/Pb zircon (Nelson 1995)|Of Bangemall Group|||Includes porphyritic rhyolite|18-NOV-11
25855|Coobarra Formation|69166|4|Described|91591.1.pdf|Paleoproterozoic|Paleoproterozoic|Age derived from sample (91591.1.pdf) (described in lithology section). dated in 1995.|1638 Ma +/- 14 Ma (SHRIMP)|Bangemall Group|||Amygdaloidal rhyolite with phenocrysts of quartz and microcline, with some phenocrysts of sanidine. Groundmass of structureless intergrowths of cryptocrystalline quartz and microcline with scattered sericite, chlorite or biotite.|08-MAR-18
25855|Coobarra Formation|70795|5|Briefly described|91591.1.pdf|Paleoproterozoic|Paleoproterozoic||1638 +/- 14 Ma|Bangemall Supergroup|||Flow banded, amygdaloidal rhyolite intercalated with conglomerates.|
75540|Coodardy Pool Formation|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Mapped as four separate but un-named units.|c.2800 Ma.|Unit in Polelle Group.|||Metamorphosed iron-formation, weakly layered, strongly foliated; medium-grained foliated quartzite; quartzite with interlayered metaperidotite schist; quartzite and metamorphosed iron-formation, well foliated.|
75540|Coodardy Pool Formation|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane||Pollelle Group|Includes 4 unnamed subunits.||Quartzite and metamorphosed iron formation; strongly foliated|
75540|Coodardy Pool Formation|69583|5|Briefly described|Plate 2|Archean|Archean|Murchison Domain. See also Coodardy Formation (p47, p49).|c.2800 Ma.|Polelle Group.|||Quartzite and metamorphosed iron-formation; strongly foliated.|
75540|Coodardy Pool Formation|69628|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton||Polelle Group|||Interlayered metamorphosed iron-formation and amphibolite schist; quartzite, medium-grained, foliated; metamorphosed iron-formation, weakly layered, strongly foliated.|17-JUL-15
75540|Coodardy Pool Formation|70796|5|Briefly described|100k_geologyl_lut.csv|Neoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, Cue100_2443_stratig.pdf, Nowthanna100_2643_stratig.pdf. Numerous additional lithologies are discussed.|ca 2800 to 2790 Ma (inferred)|Polelle Group|||Quartzite, mediumgrained, foliated; Interlayered metamorphosed iron formation and amphibolite schist.|
75540|Coodardy Pool Formation|70830|5|Briefly described|p7, p9|||||Polelle Group||Overlain by the Meekatharra Formation.|Quartzite.|
75540|Coodardy Pool Formation|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeol_lut.csv.|2800-2790 Ma|Unit of Poelle Group.||Underlain by Yaloginda Formation.|Quartzite; medium grained, foliated and metamorphosed iron formation; weakly layered, strongly foliated.|
75540|Coodardy Pool Formation|71809|5|Briefly described|map legend|Archean|Archean|Yilgarn Craton, Youanmi Terrane||Of Polelle Group.|||Garnet-mica schist with 2-5 mm euhedral garnets; commonly altered.|
75540|Coodardy Pool Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Youanmi Terrane. ||Polelle Group|||Quartzite and metamorphosed iron formation; strongly foliated.|
35000|Cooglegong Monzogranite|23046|6|Mentioned|174|||||||||
35000|Cooglegong Monzogranite|23570|5|Briefly described|p27|Archean|Archean|Age: 2851+/-2Ma.   Geological Province: Pilbara Craton||||||07-NOV-08
35000|Cooglegong Monzogranite|23783|5|Briefly described|p124|||||||||
35000|Cooglegong Monzogranite|24025|5|Briefly described|p23, p11 Tb.2|Archean|Archean|Of Shaw Granitoid Complex. Geological Province: Pilbara Craton||||||07-NOV-08
35000|Cooglegong Monzogranite|24110|5|Briefly described|Plate 1|Archean|Archean|Belongs to Shaw Granitoid Complex.  Geological Province: Pilbara Craton||||||07-NOV-08
35000|Cooglegong Monzogranite|24193|5|Briefly described|p874, p877 Tb.1|Archean|Archean|Of the Shaw granitoid complex. Geological Province: Pilbara Craton.||||||07-NOV-08
35000|Cooglegong Monzogranite|24531|4|Described|p32, p8-9 Fig. 3|Archean|Archean|Of the Shaw Granitoid Complex.  Age: c.2850Ma (zircon).||||||07-NOV-08
35000|Cooglegong Monzogranite|24532|5|Briefly described|Map legend|Archean|Archean|Of the Shaw Granitoid Complex.  Age: c.2850Ma.||||||07-NOV-08
35000|Cooglegong Monzogranite|50381|5|Briefly described|Map Legend|Archean|Archean|Of Shaw Granitoid Complex. Geological Province: Pilbara Craton. Age: 2850 Ma||||||07-NOV-08
35000|Cooglegong Monzogranite|50423|5|Briefly described|p215, Fig.1||Archean|Age: 2850 Ma.||||||07-NOV-08
35000|Cooglegong Monzogranite|50427|5|Briefly described|p186, p192 Fig.11|Archean|Archean|Age: c.2850 Ma. Of Shaw Granitoid Complex.||||||07-NOV-08
35000|Cooglegong Monzogranite|61252|6|Mentioned|p67 Tb.1|||Of the Shaw granitoid complex.||||||
35000|Cooglegong Monzogranite|61259|5|Briefly described|p403|Archean|Archean|Age: 2851+/-2Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
35000|Cooglegong Monzogranite|63441|5|Briefly described|p12 tb. 2|Archean|Archean|Intrudes Split Rock Supersuite. Supersedes Cooglegong Adamellite. Ages: 2880+/296Ma and 2877+/-20Ma. Geological province: Pilbara Craton.||||||07-FEB-11
35000|Cooglegong Monzogranite|66108|5|Briefly described|Map legend|Neoarchean|Neoarchean|Unit in Split Rock Supersuite. Monzogranite; coarse-grained and commonly porphyritic; locally fine-grained or pegmatitic; local igneous layering and flow alignment of feldspar crystals.||||||
35000|Cooglegong Monzogranite|68282|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.The 6 variants are mapped separately.|c.2850 Ma (Bickle et al. 1989).|Of the Split Rock Supersuite|||Monzogranites: leucocratic equigranular; coarse-grained to pegmatitic; coarse-grained, equigranular, biotite-; K-feldspar porphyritic to megacrystic biotite-; blue-grey mesocratic K-feldspar megacrystic; coarse-grained with common pegmatite patches.|
35000|Cooglegong Monzogranite|69012|5|Briefly described|Map Legend|Archean|Archean|Pilbara Craton. Six facies are mapped separately.||Of the Split Rock Supersuite.|||Monzogranites: coarse-grained with common pegmatite patches; K-feldspar-porphyritic to megacrystic biotite; coarse-grained equigranular biotite; coarse-grained to pegmatitic; leucocratic, fine- to medium-grained, equigranular. Greisen.|29-APR-14
35000|Cooglegong Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Leucocratic monzogranite; fine to medium grained; equigranular. Coarse grained to pegmatitic monzogranite, k-feldspar-porphyritic to megacrystic biotite monzogranite.|
35000|Cooglegong Monzogranite|69590|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Also known as Cooglegong Adamellite (hickman 1983). Events: Pilbara Craton breakup; Split Rock Supersuite Event. Sample GSWA 142879 (coarse-grained adamellite) yielded an interpreted crystallisation age of 2851+\-2 Ma (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.|2851-2831 Ma (inferred)|Unit of Split Rock Supersuite.|||Monzogranite; coarse-grained to pegmatitic, can be biotitic, K-spar megacrystic, leucocratic.|
35000|Cooglegong Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, granite, greisen|
35000|Cooglegong Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Monzogranite, coarse grained and commonly porphyritic; locally fine grained or pegmatitic; local igneous layering; metamorphosed.|
73507|Cookes Creek Monzogranite|63417|5|Briefly described|Map legend|Archean|Archean|Of Split Rock Supersuite. Geological Province: Pilbara Craton. Monzogranite, fine- to medium-grained, biotite-bearing, seriate to feldspar-phyric; intruded by quartz-barite veins.||||||07-NOV-08
73507|Cookes Creek Monzogranite|64580|4|Described|map legend||Mesoarchean|Of Split Rock Supersuite. Biotite monzogranite; seriate to feldspar porphyritic; fine to medium grained; weakly metamorphosed.||||||15-DEC-08
73507|Cookes Creek Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Biotite monzogranite; seriate to feldspar porphyritic; fine to medium grained; weakly metamorphosed.|
73507|Cookes Creek Monzogranite|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological Province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton. [Also referred to as Cookes Creek Granite on 500k_interpgeop_pilcrat02_lut.csv]. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.||Unit of Split Rock Supersuite.|||Biotite monzogranite; seriate to feldspar porphyritic; fine to medium grained; weakly metamorphosed|
73507|Cookes Creek Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; Split Rock Supersuite Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|2851-2831 Ma (inferred)|Unit of Split Rock Supersuite.|||Biotite monzogranite; seriate to feldspar porphyritic; fine to medium grained; weakly metamorphosed|
73507|Cookes Creek Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, vein barite|
73507|Cookes Creek Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||2837+/-16 Ma|Split Rock Supersuite|||Biotite monzogranite; seriate to feldspar porphyritic; fine to medium grained; weakly metamorphosed.|
35350|Coolajacka Member|24352|5|Briefly described|Map legend|Archean|Archean|Parent: Hardey Formation.   Age: ~2760Ma.   Fine-grained ultramafic lava; abundant quartz xenocrysts.  Geological Province: Hamersley Basin||||||30-JUN-14
35350|Coolajacka Member|24353|5|Briefly described|p22|Archean|Archean|Parent: Hardey Formation. Geological Province: Pilbara Craton||||||07-NOV-08
35350|Coolajacka Member|50300|5|Briefly described|Map Legend|Archean|Archean|Of the Hardey Formation.  Geological Province: Hamersley Basin. Underlies: Lyre Creek Member. Intruded by: Cooya Pooya Dolerite.||||||07-NOV-08
35350|Coolajacka Member|63372|4|Described|Map Legend|Archean|Archean|Of the Hardey Formation. Geological Province: Hamersley Basin. Underlies: Lyre Creek Member. Overlies: Hardey Formation. Fine grained ultramafic lava; abundant quartz xenocrysts.||||||07-NOV-08
35350|Coolajacka Member|69299|4|Described|p6 Tb.1, p14, p16-18, map|Archean|Archean|On COOYA POOYA, mapping indicates that both lower and upper sills of Cooya Pooya Dolerite are comagmatic with Kylena Formation, and Coolajacka Member stratigraphically underlies the Lyre Creek Member. Geol. Prov: Hamersley Basin, Pilbara Craton.||Of Hardey Formation.||Is overlain by Lyre Creek Member.|Extremely fine-grained, silicified, and pyroxene-rich ultramafic lava, with talc-chlorite pseudomorphs after orthopyroxene and olivine, and abundant quartz xenocrysts; grain size and fine spinifex texture suggests rapid cooling in ultramafic flows.|
26490|Coolbro Sandstone|22716|6|Mentioned|p239|Neoproterozoic|Neoproterozoic|||||||
26490|Coolbro Sandstone|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Throssell Group, Yeneena Basin.||||||
26490|Coolbro Sandstone|23590|3|Fully described|p9|||Of Throssell Group. Overlying unit Broadhurst Formation. Max. thickness: 4000 m.||||||
26490|Coolbro Sandstone|23594|5|Briefly described|p21|Neoproterozoic|Mesoproterozoic|See also p9 Fig. 6. Of Throssell Group. Overlying unit Broadhurst Formation. Geological Province Yeneena Basin.||||||
26490|Coolbro Sandstone|23602|4|Described|p15|||See also page 6 Table 1. Of Throssell Group. Overlain by Broadhurst Formation.||||||24-JUL-07
26490|Coolbro Sandstone|23729|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Throssell Group. Geological Province: Yeneena Basin.||||||
26490|Coolbro Sandstone|23730|4|Described|p10|Neoproterozoic|Mesoproterozoic|Of Throssell Group. Overlain by Broadhurst Formation. Geological Province: Yeneena Basin.||||||24-JUL-07
26490|Coolbro Sandstone|23742|6|Mentioned|p6|||||||||
26490|Coolbro Sandstone|23745|4|Described|p16|Neoproterozoic|Mesoproterozoic|See also page 7 Fig 5. Of Throssell Group. Geological Province: Yeneena Basin.||||||
26490|Coolbro Sandstone|23746|5|Briefly described|p8 Fig 5|Neoproterozoic|Mesoproterozoic|Of Throssell Group.||||||
26490|Coolbro Sandstone|23760|4|Described|p22|Neoproterozoic|Mesoproterozoic|Of Throssell Group. Geological Province: Yeneena Basin. Max. thickness: 4000 m.||||||
26490|Coolbro Sandstone|23780|5|Briefly described|p189|Mesoproterozoic|Mesoproterozoic|Of the Throssell Group.||||||
26490|Coolbro Sandstone|23900|4|Described|p1536|Proterozoic|Proterozoic|Of the Throssell Group. Conformably overlain by the Broadhurst Formation. Unconformably overlies the Rudall Metamorphic Complex. Geological Province: Paterson orogen.||||||24-JUL-07
26490|Coolbro Sandstone|24025|5|Briefly described|p15|Neoproterozoic|Neoproterozoic|Of the Throssell Group. Geological Province: Pilbara Craton.||||||01-DEC-11
26490|Coolbro Sandstone|24194|4|Described|p898, p899 Fig.2, p900, Fig.3|Proterozoic|Proterozoic|Of the Throssell Group. Sandstone with interbedded shale and siltstone. Overlain by  Broadhurst Formation. Geological Province: Yeneena Basin.||||||28-JUL-08
26490|Coolbro Sandstone|24594|5|Briefly described|p601|Neoproterozoic|Mesoproterozoic|Of the Throssel Group. Siliciclastic unit characterised by sericite, chlorite and hematite alteration, weakly foliated and locally brecciated. Age: 671+/-99 - 653+/-8Ma. Geological Province: Yeneena Basin (Paterson Orogen).||||||09-JUL-13
26490|Coolbro Sandstone|33849|4|Described|p124|||||||||
26490|Coolbro Sandstone|35252|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26490|Coolbro Sandstone|35902|6|Mentioned|p7|||||||||
26490|Coolbro Sandstone|36551|6|Mentioned|Table 22|||||||||
26490|Coolbro Sandstone|36632|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26490|Coolbro Sandstone|37023|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26490|Coolbro Sandstone|37212|3|Fully described|p11|||||||||
26490|Coolbro Sandstone|37214|6|Mentioned|p6|||||||||
26490|Coolbro Sandstone|37460|4|Described|Table3.VII|||||||||
26490|Coolbro Sandstone|37707|6|Mentioned|Table I|||||||||
26490|Coolbro Sandstone|42278|6|Mentioned|p33|||||||||
26490|Coolbro Sandstone|42702|5|Briefly described|map legend|Proterozoic||||||||
26490|Coolbro Sandstone|42730|5|Briefly described|p17|||Yeneena Group.||||||28-JUL-08
26490|Coolbro Sandstone|43118|4|Described|p17|||Of Yeneena Group.||||||24-JUL-07
26490|Coolbro Sandstone|43278|5|Briefly described|p644,Fig.2.||Neoproterozoic|Of Yeneena Group.||||||24-JUL-07
26490|Coolbro Sandstone|43348|3|Fully described|Table 1 p6, p9||Neoproterozoic|Of Yeneena Group.||||||24-JUL-07
26490|Coolbro Sandstone|43847|5|Briefly described|Map Legend||Proterozoic|||||||
26490|Coolbro Sandstone|43848|5|Briefly described|Map Legend||Proterozoic|||||||
26490|Coolbro Sandstone|43867|5|Briefly described|Fig.2 p201|||Shown as part of informal Lower Yeneena Sub-Group.||||||
26490|Coolbro Sandstone|44139|5|Briefly described|p277-280, p282|Neoproterozoic|Neoproterozoic|Williams et al. (1976). 4000 m. Sandstone, basal conglomerate; minor shale. Central zone of Yeneena Basin. Unconformably overlies Rudall Complex. Transitional upwards to Broadhurst Formation in Central Zone. Fluviatile or near-shore shallow-marine.| | ||||05-MAR-18
26490|Coolbro Sandstone|44189|5|Briefly described|Map legend||Proterozoic|||||||
26490|Coolbro Sandstone|44190|5|Briefly described|Map Legend||Proterozoic|||||||
26490|Coolbro Sandstone|44443|6|Mentioned|map legend|Mesoproterozoic|Mesoproterozoic|||||||
26490|Coolbro Sandstone|44831|5|Briefly described|Map Legend||Proterozoic|||||||
26490|Coolbro Sandstone|46319|5|Briefly described|p16|||Formerly Bocrabee Sandstone.||||||
26490|Coolbro Sandstone|49895|6|Mentioned|p9|||||||||
26490|Coolbro Sandstone|50544|4|Described|p56|Mesoproterozoic|Mesoproterozoic|Basal unit of the Throssell Group. Deltaic-fluviatile succession, predominantly quartz sandstone. Conformably underlies the Broadhurst Formation. Max. thickness: >200m.||||||01-DEC-11
26490|Coolbro Sandstone|50555|5|Briefly described|Map legend|Neoproterozoic||Of the Throssell Group (Yeneena Supergroup). Fine to coarse-grained sandstone; pyrite nodules common. Age: <1060Ma. Geological Province: Yeneena Basin.||||||28-JUL-08
26490|Coolbro Sandstone|60470|5|Briefly described|p4 Fig. 2, 10-11, 12-14, 15, 16|Neoproterozoic|Neoproterozoic|in Yeneena Basin, of Throssell Range Group. Unconformably overlies Rudall Complex. Transitional contact with overlying Broadhurst Formaion. Thickness 2-4 km. Sandstone; minor conglomerate, siltstone, and shale||||||
26490|Coolbro Sandstone|62453|4|Described|p5 Fig. 3, 67|Cryogenian|Cryogenian|Geological Province: Paterson Orogen. Of the Throssell Range Group. Sandstone, siltstone, conglomerate. Conformably underlies Broadhurst Formation. ||||||
26490|Coolbro Sandstone|62986|5|Briefly described|p18|Neoproterozoic|Neoproterozoic|Basal unit of the Throssell Range Group. Geological Province: Yeneena Basin.||||||25-JAN-07
26490|Coolbro Sandstone|63417|5|Briefly described|Map legend|Neoproterozoic|Mesoproterozoic|Of the Throssell Range Group. Geological Province: Yeneena Basin (Centralia Superbasin). Massive to thick-bedded quartz sandstone with minor siltstone and shale; local basal conglomerate.||||||23-JUL-07
26490|Coolbro Sandstone|64283|5|Briefly described|p54|||Of the Throssell Group. Overlain by Broadhurst Formation. Predominantly a sandy interval at base of group.||||||07-FEB-11
26490|Coolbro Sandstone|64580|4|Described|map legend||Neoproterozoic|Of Throssell Range Group. Massive to thick-bedded quartz sandstone and minor siltstone and shale; local basal conglomerate.||||||09-DEC-08
26490|Coolbro Sandstone|64725|6|Mentioned|p74.|Neoproterozoic|Neoproterozoic|||Unit in Throssell Range Group.||Unconformably overlies Rudall Complex.||
26490|Coolbro Sandstone|64777|4|Described|p3 Fig.4, p4-8|Neoproterozoic|Neoproterozoic|Fluvial-deltaic succession up to 4km thick. SHRIMP U-Pb ages. Detrital zircon populations at 1780 Ma, 1310-1000 Ma, and a minor group from 1670 to 1310 Ma. |Max. deposition 950 Ma (Bagas and Nelson 2007).|Of the Throssell Range Group|||Fine-to coarse-grained, cross-bedded and graded sandstone, interbedded with locally common conglomerate and siltstone.|
26490|Coolbro Sandstone|64941|5|Briefly described|p27, p29|Tonian|Tonian|Yeneena Basin. Age: c. 980 Ma, maximum depositional age, SHRIMP U-Pb detrital zircon.|see comments|Throssell Range Group.||Is overlain by Malu Formation, and Broadhurst Formation||
26490|Coolbro Sandstone|64943|5|Briefly described|p17, p8, 14, 17, 20, 30, 29,35,37,39|Neoproterozoic|Neoproterozoic|Of Throssell Group. Forms fault bounded wedges in Clayton Domain. Paleocurrent data supports sediment transport from SW. Significantly deformed by only D4. Fluviodeltaic clastic rocks.||||||
26490|Coolbro Sandstone|65403|5|Briefly described|p13.|||||Basal unit of Throssell Group.||Is conformably overlain by Broadhurst Formation.|Sandstone and conglomerate.|
26490|Coolbro Sandstone|65454|4|Described|p7-8, p10-11, p19, p23, p30 Fig.A1b|Cryogenian|Tonian|Yeneena Basin. Of Throssell Range Group. Regionally extensive massive sandstone; minor siltstone, shale and carbonate. Basal conglomerate in some areas. Fluviatile. Up to 2.5 km thick. Max dep age of 910 Ma. Correlated with Choorun Formation and Gunanya Sandstone.||||||
26490|Coolbro Sandstone|65725|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Throssell Range Group. Overlain by Broadhurst Formation. Massive to thick-bedded quartz sandstone. Minor siltstone and shale. Age <1070 Ma and older than Miles Orogeny (c.720 Ma). Province: Yeneena Basin (Centralian Superbasin)||||||26-FEB-13
26490|Coolbro Sandstone|65826|4|Described|p1, p12, p14. |Neoproterozoic|Neoproterozoic|The Miles Orogeny produced NW-trending folds and faults. Fractured and sheared sandstones may contain significant groundwater supplies.||Basal unit in Throssell Range Group.||Unconformably overlies Rudall Complex. Is overlain conformably by Broadhurst Formation.|Fine- to coarse-grained, massive to well-bedded quartz sandstone, with recrystallized quartz grains; minor siltstone and shale interbeds, poorly exposed, commonly sheared and veined by quartz; rare ripple marks and cross-lamination.|
26490|Coolbro Sandstone|67182|6|Mentioned|p677 Fig.2, p678|Neoproterozoic|Neoproterozoic|Of the Yeneena Basin. 910 Ma is age of the youngest detrital zircon (Bagas and Nelson 2007), 830 Ma is the age of intermediate to mafic rocks that intrude the lower part of the (Yeneena) Basin (Maidment, unpublished). See also Coolbro Formation (p678).|ca 910-830 Ma|||Unconformably overlies Yandagooge Formation||
26490|Coolbro Sandstone|67202|3|Fully described|p1, p4-5, p53, p57-58, p61-63, p65,|Neoproterozoic|Neoproterozoic|See also  p93-94, p115, p117, p132, p134, p136-138, p149-150, p155-157, p161-165, p170-171, p174, p177-179, p181-187, p203, p219, p221, p229, p231, p233-235, p237-247, p249-250, p253, p272-273, p277-279, p281. Yeneena Basin. Up to 3-4km thick; regionally extensive. Basal unconformity is associated with uranium mineralisation. Hosts Sunday Creek and Mount Sears U prospects at/near contact with Broadhurst Formation (described in detail). Fluvio-deltaic deposits up to 4km thick sourced from adjacent Rudall Complex. Generalised lithological column. Gravity and aeromagmetic interpretation; conductivity models and images. Geochemistry discussed. Appears also as Coolbro Formation on p155.|<910 Ma (maximum depositional age).|Throssell Range Group.||Overlies Pungkuli Formation, and unconformably the Rudall Complex. Is overlain transitionally by Broadhurst Formation. Correlated with Gunanyah Sandstone; corresponds with Heavitree Sandstone.|Mainly fine- to coarse-grained sandstone; siltstone lenses in upper parts.|15-FEB-18
26490|Coolbro Sandstone|67430|6|Mentioned|p21-22|||Yeneena Basin. Appears also as Coolbro Formation (p21). Minimum age (intrusions) is ~830 Ma.|~910 Ma (MDA).|||Unconformably overlies Yandagooge Formation.||
26490|Coolbro Sandstone|69003|6|Mentioned|p60-61, p64|Neoproterozoic|Neoproterozoic|Basal unit in the Yeneena Basin, NW Paterson Orogen. Multiple 40Ar/39Ar muscovite ages date the Miles Orogeny at c.655 Ma.||Throssell Range Group.||||
26490|Coolbro Sandstone|69167|4|Described|geologyp_lut.csv|Neoproterozoic|Mesoproterozoic|Age derived from quartz rich metasandstone sample (172840.1.pdf) and constrains maximum age for deposition of sandstone protolith.|2710 +/- 31 Ma (SHRIMP)|Throssell Range Group||Underlies Broadhurst Formation|Massive to thick-bedded quartz sandstone and minor siltstone and shale; local basal conglomerate|
26490|Coolbro Sandstone|69590|4|Described|250k_interpgeop_lut.csv|Cryogenian|Neoproterozoic|Geological province: Paterson Orogen. Of Yeneena Basin. Events: Miles Orogeny; Paterson Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|911-650 Ma (inferred)|Unit of Throssell Range Group.|||Massive to thick-bedded quartz sandstone and minor siltstone and shale; local basal conglomerate|
26490|Coolbro Sandstone|71080|6|Mentioned|p26|||Yeneena Basin. Probable Tonian age.||Of Throssell Range Group||||
26490|Coolbro Sandstone|71169|5|Briefly described|p11 fig 10, p15|Neoproterozoic|Neoproterozoic|Yeneena Basin.|||||Feldspathic arenite.|
26490|Coolbro Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone, pelite, crystalline carbonate|
26490|Coolbro Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Cryogenian|Tonian|Yeneena Basin.|Max age 911+/-23 Ma.|Throssell Range Group.|||Massive to thick-bedded quartz sandstone and minor siltstone and shale; local basal conglomerate.|
77855|Coolgardie Subgroup|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2726 - 2699 Ma (inferred).|Kalgoorlie Group|Includes Gleesons Basalt, Hampton Hill Formation, Lindsays Basalt, Brilliant Formation, Burbanks Formation, Greenmont Basalt.|||
77855|Coolgardie Subgroup|71270|5|Briefly described|GEOL_LUT_CSV files|||Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.||Unit of Kalgoorlie Group.|Includes Brilliant Formation; Burbanks Formation, Gleesons Basalt, Greenmont Basalt, Hamption Hill Formation, Lindsays Basalt.|Intruded by Tindals Diorite.||
77855|Coolgardie Subgroup|72095|6|Mentioned|p5 Fig 3|Neoarchean|Neoarchean|Eastern Goldfields, Yilgarn Craton.||Unit of Kalgoorlie Group.||||
77855|Coolgardie Subgroup|73596|6|Mentioned|p1162|||Coolgardie Inlier, Kalgoorlie Terrane.|||Lindsays, Gleesons Basalts; Hampton Hill Formation.|Overlies Brilliant Formation. Is overlain by Black Flag Group.||
80097|Coolyena Group, Lower|70826|6|Mentioned|p7 tbl 4|Cretaceous|Cretaceous|Perth Basin.||||||
80103|Coolyena Group, Upper|70826|6|Mentioned|p7 tbl 4|Cretaceous|Cretaceous|Perth Basin.||||||
80808|Coolyena Megasequence|71958|5|Briefly described|p40-p41, p45,46, 48, p54, p62, p74|Maastrichtian|Aptian|Vlaming Sub-basin. Sequence stratigraphy.Shallow marine shelfal succession shallow  deposited during the post-breakup thermal subsidence. Corresponds to the Cretaceous Megasequence 6 of Nicholson et al. (2008).||||||07-MAR-19
38602|Coolyia Creek Granodiorite|23783|5|Briefly described|p113|Archean|Archean|Age: c. 3467 Ma.||||||15-APR-13
38602|Coolyia Creek Granodiorite|50381|5|Briefly described|Map Legend|Archean|Archean|Of Shaw Granitoid Complex. Geological Province: Pilbara Craton. Age: c. 3469 Ma||||||07-NOV-08
38602|Coolyia Creek Granodiorite|50423|5|Briefly described|p215, Fig.1||Archean|Age: c. 3470 Ma. Of North Shaw Suite.||||||07-NOV-08
38602|Coolyia Creek Granodiorite|50427|5|Briefly described|p186|Archean|Archean|Age: 3468 Ma. Intrudes base of Warrawoona Group. Of Shaw Granitoid Complex.||||||07-NOV-08
38602|Coolyia Creek Granodiorite|63441|5|Briefly described|p7 Tb. 2|Archean|Archean|Of the North Shaw Suite. Age: 3469 +/-2 Ma. Geological province: Pilbara Craton.||||||15-APR-13
38602|Coolyia Creek Granodiorite|64621|5|Briefly described|Map legend|Archean|Archean|Of the Callina Supersuite. Age: c. 3469Ma. Metagranodiorite to metatonalite; clotty hornblende texture, strongly foliated.||||||15-APR-13
38602|Coolyia Creek Granodiorite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Callina Supersuite. Aged c. 3469 Ma. Metagranodiorite to metatonalite; clotty hornblende textured; strongly foliated.||||||15-APR-13
38602|Coolyia Creek Granodiorite|69012|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane.|3469-3467 Ma (McNaughton et al., 1988)|Of the Callina Supersuite.|||Comprises metagranodiorite to metatonalite; clotty hornblende texture; strongly foliated.|
38602|Coolyia Creek Granodiorite|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Geochronology by Zeegers (1996) and McNaughton et al (1998). |3469-3467 Ma||||Metagranodiorite to metatonalite; clotty hornblende textured; strongly foliated.|01-MAY-14
38602|Coolyia Creek Granodiorite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Callina Supersuite|||Metagranodiorite to metatonalite; clotty hornblende texture; strongly foliated|
38602|Coolyia Creek Granodiorite|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA 142962 (tonalite) yielded an interpreted igneous crystallisation age of 2469+\-2 Ma  (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.|3493-3467 Ma (Isotopic)|Unit of North Shaw Suite.|||Metagranodiorite to metatonalite; clotty hornblende texture; strongly foliated|
38602|Coolyia Creek Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite|
38602|Coolyia Creek Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||3469+/-2 Ma.|Callina Supersuite|||Metagranodiorite to metatonalite; clotty hornblende texture; strongly foliated.|
37866|Coomb Bore Monzogranite|24530|4|Described|p21|Archean|Archean|Age: 2691+/-3Ma and 2686+/-5Ma.  Geological Province: Yilgarn Craton.  See also p6 Fig. 3.||||||07-NOV-08
37866|Coomb Bore Monzogranite|50012|5|Briefly described|Map|Archean|Archean|Foliated monzogranite.  Age: c.2691Ma. Geological Province: Yilgarn Craton||||||07-NOV-08
37866|Coomb Bore Monzogranite|50293|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Yilgarn Craton.  Age: c.2686Ma.||||||07-NOV-08
37866|Coomb Bore Monzogranite|65269|5|Briefly described|p8 Fig.5, p23-24, p25, p29-30|Neoarchean|Neoarchean|A small NW elongated intrusion; in the Edale Shear Zone; monzogranite with minor syenogranite and granodiorite; typically medium-grained, equigranular to porphyritic; SHRIMP U-Pb zircon crystallisation ages of 2691+/-3 and 2686+/-5 Ma||||||
37866|Coomb Bore Monzogranite|69583|5|Briefly described|Plate 2|Archean|Archean||c.2690 Ma.||||Foliated monzogranite, metamorphosed.|
37866|Coomb Bore Monzogranite|70153|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean||2691 +/- 3 Ma - 2686 +/- 5 Ma (isotopic).||||Medium- to coarse-grained, foliated metamonzogranite; includes minor syenogranite and granodiorite.|
37866|Coomb Bore Monzogranite|70796|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton.|2691 +/ 3 Ma to 2686 +/ 5 Ma (isotopic)||||Medium to coarsegrained, foliated metamonzogranite; includes minor syenogranite and granodiorite|
37866|Coomb Bore Monzogranite|71269|4|Described|500k_interpgeop16_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma). |2691+\-3 Ma; 2686+\-5 Ma||||Medium- to coarse-grained, foliated metamonzogranite; includes minor syenogranite and granodiorite|
37866|Coomb Bore Monzogranite|71270|4|Described|500k_interpgeop16_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2691+\-3 Ma; 2686+\-5 Ma||||Medium- to coarse-grained, foliated metamonzogranite; includes minor syenogranite and granodiorite|
37866|Coomb Bore Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||Max age 2691+/-3 Ma, min 2686+/-5 Ma.||||Medium- to coarse-grained, foliated metamonzogranite; includes minor syenogranite and granodiorite.|
68055|Coondamar Formation|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Of the Nullagine Group. Geological Province: eastern Pilbara Craton.||||||07-NOV-08
68055|Coondamar Formation|61264|5|Briefly described|p62|Archean|Archean|Of the Nullagine Group (De Grey Supergroup). Conformably overlain by Mosquito Creek Formation. Geological Province: Mosquito Creek Basin/Pilbara Craton.||||||07-NOV-08
68055|Coondamar Formation|63417|5|Briefly described|Map legend|Archean|Archean|Of Nullagine Group (De Grey Supergroup). Geological Province: Pilbara Craton. Metamorphosed siliciclastic and mafic igneous rocks.||||||07-NOV-08
68055|Coondamar Formation|63441|4|Described|p5 Tb.1, p29|Archean|Archean|Of Nullagine Group (De Grey Supergroup). Conformably overlain by Mosquito Creek Formation. Lithic sandstone containing subangular basaltic clasts; northern section comprises chloritic metasedimentary rocks, metachert, metagabbro and amphibolite.||||||07-FEB-11
68055|Coondamar Formation|63538|4|Described|p7, p6 Fig. 3|Archaean|Archaean|Underlies Mosquito Creek Formation. Mafic schists and fine-grained metasedimentary rocks with dominantly mafic detritus. Geological Province: Pilbara Craton.||||||19-APR-13
68055|Coondamar Formation|63854|5|Briefly described|p229-234, p236.|Mesoarchean|Mesoarchean|Thickness >1 km. Poorly-constrained age between c.3200 and 2938 Ma (Bagas, 2005). Deformation described. Hosts gold dated 2905 +/- 9 Ma (Pb-Pb model ages on epigenetic galena; Huston et al., 2002a).|Minimum age 2905 +/- 9 Ma.|Of Nullagine Group.||Conformably overlain by Mosquito Creek Formation.|Lithic sandstone with basaltic clasts in the north; chloritic metasedimentary rocks, metachert, metagabbro, metamorphosed mafic and ultramafic rocks in the south.|
68055|Coondamar Formation|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of De Grey Group. Geological Province: Pilbara Craton. Consists of layred chert, schist, siltstone, foliated sandstone and silstone, basalt, gabbro and sandstone, all metamorphosed. See map legend for more information.||||||07-FEB-11
68055|Coondamar Formation|64656|5|Briefly described|Map Legend|Archaean|Archaean|Of Nullagine Group. Geological Province: Pilbara Craton.||||||26-NOV-08
68055|Coondamar Formation|65008|5|Briefly described|p8 Fig.8, p16-18, p19 Fig.14, p41|||Mosquito Creek Basin. Includes 9 separately mapped facies. ~1km thick.||Of the De Grey Group||Unconformably underlain by the Paddy Market Formation?|Chlorite-actinolite schist, mica schist and amphibolite; metasedimentary rock; local metamorphic rocks; undivided, east of Meentheena Fault Zone.|
68055|Coondamar Formation|65825|4|Described|p6, pp12-14, p19,  pp32-33.|Archean|Archean|Mosquito Creek Basin. Named after Coondamar Creek in the map area. Type area southwest of Hallcomes Peak. A basal sediment-mafic-ultramafic succession. A subdivision of the Mosquito Creek Formation as defined by Hickman (1978); now separated on the bases of new geochronological data and field mapping. Appendix 2 shows this as a unit of the Nullagine Group in the De Grey Supergroup, according to the GSWA databases. Equivalent to the informally named Middle Creek Formation of Blewett et al. (2002). Mapped as 17 un-named sub-units which are each described in this report. A small diorite intrusion, one of several such mafic plugs, had a zircon crystal dated 3035 +/- 6 Ma, which further constrains the minimum age. Hosts sub-economic base metal mineralization.|Between c.3315 Ma and c.2926 Ma.|||Is paraconformably overlain by Mosquito Creek Formation.|Metamorphosed and multiply-deformed sandstone and siltstone; minor chert, basalt, gabbro, ultramafic rock and felsic rock; metamorphosed to amphibolite, tremolite-actinolite schist, quartz-muscovite schist, semipelitic schist.|
68055|Coondamar Formation|65828|5|Briefly described|Map legend|Archean|Archean|||Unit in De Grey Group.||Locally interleaved with Golden Eagle Orthogneiss.|Wide range of lithologies including chlorite-actinolite schist, quartz-muscovite schist, amphibolite, phyllite; layered chert, typically ferruginised; metamorphosed siltstone, minor sandstone, basaltic lithic sandstone, gabbro and ultramafics.|
68055|Coondamar Formation|66217|5|Briefly described|p40.|||Base of the Mosquito Creek Basin.|<3200 Ma.|||Is overlain by Mosquito Creek Formation.|Mixed assemblage of siliciclastic and mafic and ultramafic volcanic and intrusive rocks.|10-JUN-20
68055|Coondamar Formation|67201|4|Described|p12 Tb.1, p23|||In Pilbara Craton, Coondamar Basin, rift-related successions. Tectonic contact at base. Previously Mosquito Creek Formation was defined as single, predominantly clastic sedimentary unit in Mosquito Basin by Hickman (1978, 1983), although noted lowermost 1000 m is mixed package of metamorphosed clastic sedimentary rocks and mafic and felsic volcanic rocks intruded by ultramafic-mafic sills. Farrell (2006) divided the Mosquito Basin into Coondamar Formation (lower succession of mafic-ultramafic rocks and associated sedimentary rocks) and remainder of basin fill within Mosquito Formation.|c. 3200 Ma|||Unconformably overlies Warrawoona Group.|Mafic-ultramafic rocks and associated sedimentary rocks.|
68055|Coondamar Formation|68035|6|Mentioned|p289|||On NW margin of Kurrana Terrane.?shallow-water clastic successions and thick volcanic piles, in passive margin settings.|?3202 - 3165 Ma|||||
68055|Coondamar Formation|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|Intruded by unnamed granodiorite sill and pegmatite veins with ages of 3292+/-15 Ma and 1793+/- 17 Ma respectively.||Nullagine Group|||Schist and amphibolite, foliated interlayered psammite and pelite; typically chloritic; Metasiltstone and metasandstone; chlorite bearing;  Pelitic and semipelitic schist, metagabbro, metaperidotite. Pebble and cobble conglomerate.|
68055|Coondamar Formation|69301|4|Described|p9 Tb.1, p13, p16|||Pilbara Craton. Uncertain age and lithostratigraphic relationships. Shown in Tb.1 as possible in either Mosquito Creek Basin or Coondamar (Sub-)Basin. In this paper, Coondamar Formation is interpreted to occupy lower section of Mosquito Creek Basin. It is interleaved with 3.18 Ga granitic rocks of Kurrana Terrane, suggesting a depositional age >3.18 Ga. However, this formation has not been dated directly, and may include rocks of various ages.|see comments|||Is overlain by Mosquito Creek Formation.|A deformed and metamorphosed assemblage of sedimentary and volcanic rocks.|
68055|Coondamar Formation|69590|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton. Of Mosquito Creek Basin. Events: Mosquito Creek Orogeny. Sample GSWA 178203 (biotite granodiorite) intrudes into Coondamar Formation and yielded an interpreted maximum igneous crystallisation age of 3035+\-6 Ma (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv.|3200-2980 Ma (inferred)|Unit of Nullagine Group.||Locally interleaved with Golden Eagle Orthogneiss.|Amphibolite, chlorite-actinolite schist, quartz-muscovite schist, pelitic schist, foliated interlayered psammite and pelite, layered chert, metasandstone, measiltstone, conglomerate, metagabbro, metamorphosed ultramafic intrusive rocks.|
68055|Coondamar Formation|70775|5|Briefly described|p12|||Coondamar Basin.||||||
68055|Coondamar Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||mafic schist, felsic schist, amphibolite, pelite|
68055|Coondamar Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mosquito Creek Basin.||Nullagine Group|||Metamorphosed siliciclastic and mafic igneous rocks.|
68055|Coondamar Formation|72668|5|Briefly described|p4, p15, p22|||South eastern Pilbara Craton. Similar to the lower part of the De Grey Supergroup. In fault contact with the Kurrana Terrane. Includes base metal mineralisation dated at 2905+/-9 Ma (basin deformation age?), and synchronous with Au mineralisation in Mosquito Creek Formation.||Nullagine Group.||Overlain by the Mosquito Creek Formation.|Dominantly mafic schists and fine-grained metasedimentary rocks with dominantly mafic detritus. Felsic volcanic schists and ferruginous chert is also present.|12-JAN-22
38011|Coondina Monzogranite|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Of Shaw Granitoid Complex. Geological Province: Pilbara Craton.||||||15-APR-13
38011|Coondina Monzogranite|24110|5|Briefly described|Plate 1|Archean|Archean|Belongs to Shaw Granitoid Complex. Geological Province: Pilbara Craton.||||||15-APR-13
38011|Coondina Monzogranite|24193|5|Briefly described|p874, p875 Fig.2, p877 Tb.1|Archean|Archean|Parent: Shaw granitoid complex. Geological Province: Pilbara Craton.||||||07-NOV-08
38011|Coondina Monzogranite|24531|5|Briefly described|p29, p8-9 Fig. 3|Archean|Archean|Of the Shaw Granitoid Complex. Age: c. 2936 Ma. Intrudes the Garden Creek Monzogranite; intruded by small plutons of Mulgandinnah Monzogranite.||||||15-APR-13
38011|Coondina Monzogranite|24532|5|Briefly described|Map legend|Archean|Archean|Of the Shaw Granitoid Complex. Age: >2929 Ma.||||||15-APR-13
38011|Coondina Monzogranite|50427|5|Briefly described|p187 Fig.8|Archean|Archean|Age: ?2930 Ma. Of Shaw Granitoid Complex.||||||07-NOV-08
38011|Coondina Monzogranite|63441|5|Briefly described|p11 Tb. 2|Archean|Archean|Of Sisters Supersuite. Supersedes Coondina Adamellite. Geological Province: Pilbara Craton.||||||15-APR-13
38011|Coondina Monzogranite|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Sisters Supersuite. Geological Province: Pilbara Craton. Medium-grained, weakly porphyritic biotite monzogranite.||||||
38011|Coondina Monzogranite|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Unit in Sisters Supersuite. Biotite monzogranite; leucocratic; medium-grained to weakly porphyritic.||||||
38011|Coondina Monzogranite|68282|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|c.2933-c.2927 Ma|Of the Sisters Supersuite|||Biotite monzogranite; leucocratic; medium grained to weakly porphyritic.|03-DEC-14
38011|Coondina Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Sisters Supersuite|||Biotite monzogranite; leucocratic; medium-grained to weakly porphyritic.|
38011|Coondina Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; North Pilbara Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|2954-2919 Ma (inferred)|Unit of Sisters Supersuite.|||Biotite monzogranite; leucocratic; medium-grained to weakly porphyritic|
38011|Coondina Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, granite|
38011|Coondina Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Sisters Supersuite|||Biotite monzogranite; leucocratic; medium grained to weakly porphyritic.|
28471|Coondiner Member|33544|6|Mentioned|p89|||Informal name. Lower part of Weeli Wolli Formation||||||
28471|Coondiner Member|71808|6|Mentioned|p40|||Obsolete name for the basal part of the Weeli Wolli Formation when it was included in the Brockman Iron Formation.||||||
25677|Coondra Formation|22589|6|Mentioned|p125||Proterozoic|||||||
25677|Coondra Formation|22816|5|Briefly described|p8 Table 1|||Savory Group||||||
25677|Coondra Formation|22901|6|Mentioned|76 fig 2|||Geol province Officer Basin||||||
25677|Coondra Formation|22907|6|Mentioned|42|||Geol province Officer Basin. Parent Sunbeam Group.||||||
25677|Coondra Formation|23156|6|Mentioned|p16|||From ROBERSTON map sheet.||||||
25677|Coondra Formation|23557|5|Briefly described|p95 Fig.1|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||
25677|Coondra Formation|23729|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Savory Group. Geological Province: Savory Basin.||||||
25677|Coondra Formation|23730|4|Described|p12|Neoproterozoic|Neoproterozoic|Of Sunbeam Group. Overlying unit Mundadjini Formation. Geological Province: Officer Basin.||||||
25677|Coondra Formation|24594|5|Briefly described|p602|Neoproterozoic|Neoproterozoic|Sandstone/conglomerate unit. of the Sunbeam Group.  Unconformably overlies the Ruddall Complex.  Geological Province: Officer Basin (Paterson Orogen).||||||
25677|Coondra Formation|41669|4|Described|p50|||||||||
25677|Coondra Formation|41768|2|Defined|Table 5|Precambrian||||||||
25677|Coondra Formation|42708|5|Briefly described|Plate 1|Proterozoic||||||||
25677|Coondra Formation|43055|4|Described|p29, Table 4|||Of Savory Group.||||||30-SEP-08
25677|Coondra Formation|43056|5|Briefly described|Map Legend|||of Savory Group||||||
25677|Coondra Formation|43756|4|Described|Fig.1,p535-37,540-1|||||||||
25677|Coondra Formation|44111|6|Mentioned|p.58|||in Savory Basin. Is lithologically similar to Googhenama Formation (Paterson Orogen) and Townsend Quartzite (Officer Basin).||||||
25677|Coondra Formation|50008|5|Briefly described|p46 Fig.3|Neoproterozoic||Of Sunbeam Group. Geological Province: Officer Basin.||||||
25677|Coondra Formation|61732|5|Briefly described|p4 Fig. 3, p58 Fig. 22|Willouran|Willouran|Of the Sunbeam Group. Geological Province: northwestern Officer Basin.||||||07-FEB-11
25677|Coondra Formation|62453|3|Fully described|p5 Fig. 3, 12 Fig. 8, 53|Cryogenian|Tonian|Of the Sunbeam Group. Geological Province: Officer Basin. Previously part of Calyie Sandstone. Thickness ~1000m. Conglomerate and sandstone. Conformably overlies Watch Point Formation. Disconformably overlain by Mundadjini Formation.||||||30-SEP-08
25677|Coondra Formation|62987|5|Briefly described|p30|Neoproterozoic|Neoproterozoic|Of the Sunbeam Group. Geological Province: Officer Basin.||||||
25677|Coondra Formation|64580|4|Described|map legend||Neoproterozoic|Of Sunbeam Group. Coarse-grained sandstone, pebble to boulder conglomerate.||||||09-DEC-08
25677|Coondra Formation|64625|6|Mentioned|p258|||Savory Sub-basin (Western Officer Basin). Contains mafic sills of similar composition and age to those in the Bitter Springs Formation (Amadeus Basin).||||||
25677|Coondra Formation|64772|5|Briefly described|p15|Neoproterozoic|Neoproterozoic|Of the Sunbeam Group. Geological province: Officer Basin.||||||07-FEB-11
25677|Coondra Formation|64793|6|Mentioned|p283 fig 2|Cryogenian|Cryogenian|Of NW Officer Basin.||||||
25677|Coondra Formation|65338|6|Mentioned|p59.|||Savory Basin. Considered by Walter and Veevers (2000) to correlate with Vaughan Springs Quartzite.||||||
25677|Coondra Formation|65363|6|Mentioned|p5 Fig.4. |Neoproterozoic|Neoproterozoic|||||||
25677|Coondra Formation|65365|5|Briefly described|p10 Fig. 4|Cryogenian|Cryogenian|Northwestern Officer Basin||||||
25677|Coondra Formation|65366|5|Briefly described|p23 Fig. 3|Cryogenian|Cryogenian|Northwestern Officer Basin||||||
25677|Coondra Formation|68733|6|Mentioned|p190|||Western Officer Basin.||||||
25677|Coondra Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|NW Officer Basin.||||||
25677|Coondra Formation|69185|4|Described|500k_geologyp08_lut.csv||Neoproterozoic|Of Officer Basin.||Unit of Sunbeam Group.|||Coarse-grained sandstone, pebble to boulder conglomerate|
25677|Coondra Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
25677|Coondra Formation|72034|5|Briefly described|500k_interpgeop16_lut|Tonian|Tonian|Blake Sub-basin, Officer Basin (Phase 1).||Sunbeam Group|||Coarse-grained sandstone, pebble to boulder conglomerate.|
69683|Coongan Subgroup|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup).  Geological Province: eastern Pilbara Craton.||||||07-NOV-08
69683|Coongan Subgroup|63417|5|Briefly described|Map legend|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup).  Includes Mount Ada Basalt and Duffer Formation (age: c.3465Ma). Geological Province: Pilbara Craton.||||||07-NOV-08
69683|Coongan Subgroup|63420|5|Briefly described|Map legend|Archean|Archean|Of Warrawoona Group (Pilbara Supergroup).  Includes Mount Ada Basalt and Duffer Formation. Ages: c.3469Ma and 3474-3463Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
69683|Coongan Subgroup|63441|4|Described|p4 Tb. 1, p19|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Comprises Mount Ada Basalt and Duffer Formation, both formerly of Talga Talga Subgroup. Overlies Talga Talga Subgroup. Max. thickness: 8000m in type area. Geological province: Pilbara Craton.||||||07-FEB-11
69683|Coongan Subgroup|63538|4|Described|p5, p6 Fig. 3|Archean|Archean|Of Warrawoona Group. Includes Duffer Formation and Mount Ada Basalt. Age: 3474-3463 Ma. Geological Province: Pilbara Craton. Mafic volcanic rocks.||||||19-APR-13
69683|Coongan Subgroup|64405|5|Briefly described|p2 Fig. 1|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Geological province: East Pilbara Terrane.||||||07-FEB-11
69683|Coongan Subgroup|64580|6|Mentioned|map legend|||||||||
69683|Coongan Subgroup|64621|5|Briefly described|Map legend|Archean|Archean|Of the Warrawoona Group. Contains Duffer Formation and Mount Ada Basalt.  Comprehensive lithological details included.||||||07-NOV-08
69683|Coongan Subgroup|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c.3469 - c.3465 Ma.|Of Warrawoona Group.|Includes Mount Ada Basalt and Duffer Formation.|||
69683|Coongan Subgroup|65827|4|Described|p8, p16-17|Paleoarchean|Paleoarchean|Of redefined (Van Kranendonk et al. 2006) Warrawoona Group; includes basal Mount Ada Basalt and overlying Duffer Formation. 3474-3430 Ma. Overlain by Salgash Subgroup.||||||21-JAN-22
69683|Coongan Subgroup|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Warrawoona Group. Includes Mount Ada Basalt and Duffer Formation. ||||||
69683|Coongan Subgroup|66217|4|Described|p5, p6 Table 1, p14, pp17-24.|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Mount Ada Basalt was assigned to this Subgroup by Van Kranendonk et al. (2006a). Thickness to 8200 m.|3477-3463 Ma (Van Kranendonk et al. 2006a).|Unit in Warrawoona Group.|Includes Mount Ada Basalt and Duffer Formation.|Conformably overlies Talga Talga Subgroup. Is overlain paraconformably by Salgash Subgroup, and unconformably by Gorge Creek Group and Strelley Pool Formation.||
69683|Coongan Subgroup|66664|5|Briefly described|p3.  |||East Pilbara Terrane||Unit in Warrawoona Group.||Overlies Talga Talga Subgroup. Is overlain by Salgash Subgroup.||
69683|Coongan Subgroup|66745|5|Briefly described|p54 Fig.4.|Paleoarchean|Paleoarchean|||Unit in Warrawoona Group.|Includes Mount Ada Basalt and Duffer Formation.|Disconformably overlies Talga Talga Subgroup. Is disconformably overlain by Salgash Subgroup.||
69683|Coongan Subgroup|67197|5|Briefly described|p3-4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Warrawoona Group.|Mount Ada Basalt, Duffer Formation.|||
69683|Coongan Subgroup|67201|4|Described|p7 Fig.4|||In northern Pilbara Craton, East Pilbara Terrane.||Warrawoona Group|Duffer Formation, Mount Ada Basalt|||
69683|Coongan Subgroup|67269|5|Briefly described|p6 Fig.3|Paleoarchean|Paleoarchean|||Warrawoona Group.|Mount Ada Basalt; Duffer Formation.|Overlies Talga Talga Subgroup. Is overlain by Salgash Subgroup.||
69683|Coongan Subgroup|67270|5|Briefly described|p3-4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Warrawoona Group.|Mount Ada Basalt, Duffer Formation.|Overlies Dresser Formation. Is overlain by Salgash Subgroup.||
69683|Coongan Subgroup|68035|4|Described|p288 Fig 4|Paleoarchean|Paleoarchean|Pilbara Supergroup, East Pilbara Terrane.|C3470-3463 Ma|Of Warrawoona Group. |Includes Mount Ada Basalt, Duffer Formation.|Disconformably overlies Talga Talga Subgroup. Disconformably overlain by Salgash Subgroup.|Basalt, felsic volcanics, lesser jaspilite, komatiitic basalt, siliciclastic rocks.|
69683|Coongan Subgroup|68280|6|Mentioned|p4|||||Warrawoona Group|Includes Mount Ada Basalt, Duffer Formation|||
69683|Coongan Subgroup|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|<3477-c.3463 Ma.|Of the Warrawoona Group.|Includes Duffer Formation, Mount Ada Basalt.|||02-DEC-14
69683|Coongan Subgroup|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Warrawoona Group.|Includes Duffer Formation, Mount Ada Basalt.|||19-JUN-14
69683|Coongan Subgroup|68284|5|Briefly described|p7|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Warrawoona Group.|Duffer Formation, Mount Ada Basalt.|Overlies Talga Talga Subgroup. Is overlain by Salgash Subgroup.||
69683|Coongan Subgroup|69012|5|Briefly described|Map Legend|Archean|Archean||3470-3463 Ma.|Of the Warrawoona Group.|Includes Duffer Formation and Mount Ada Basalt.|||28-APR-14
69683|Coongan Subgroup|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. |c.3477-c.3458 Ma.|Of the Warrawoona Group.|Includes the Duffer Formation and Mount Ada Basalt.|||02-MAY-14
69683|Coongan Subgroup|69167|6|Mentioned|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Warrawoona Group|Includes Duffer Formation, Mount Ada Basalt|||
69683|Coongan Subgroup|69185|5|Briefly described|500k_geologyp08_lut.csv|||Geological Province: Pilbara Craton.||Unit of Warrawoona Group.|Includes Duffer Formation.|||
69683|Coongan Subgroup|69301|5|Briefly described|p5 Fig.3|||Pilbara Craton. East Pilbara Terrane.||Warrawoona Group|Duffer Formation, Mount Ada Basalt|Disconformity at base and top.||
69683|Coongan Subgroup|69590|5|Briefly described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 250k_interpgeol_lut.csv.||Unit of Warrawoona Group.|Includes Duffer Formation, Mount Ada Basalt.|||
69683|Coongan Subgroup|70022|6|Mentioned|p115|||East Pilbara Terrane.||Warrawoona Group.|Mount Ada Basalt, Duffer Formation.|||
69683|Coongan Subgroup|70729|6|Mentioned|p164|||Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawoona Group.||||
69683|Coongan Subgroup|70733|6|Mentioned|p105|||Eastern Pilbara Craton.||Warrawoona Group.||||
69683|Coongan Subgroup|70884|5|Briefly described|p123,125,136|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawoona Group.|Includes Marble Bar Chert Member, Duffer Formation and Mount Ada Basalt.|Overlain by Warrawoona Group/Apex Basalt. Underlain by Talga Talga Subgroup/Mc Phee Formation.||
69683|Coongan Subgroup|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||acid volcanic rock, felsic schist, basalt, dacite|
69683|Coongan Subgroup|71487|5|Briefly described|p128|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawonna Group.||Overlain by Salgash Subgroup. Underlain by Talga Talga Subgroup.||
69683|Coongan Subgroup|72034|6|Mentioned|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Duffer Formation, Mount Ada Basalt.|||
69683|Coongan Subgroup|72251|5|Briefly described|p54|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawonna Group.|Includes Duffer Formation and Mount Ada Basalt.|Overlain by Salgah Subgroup. Underlain by Talga Talga Subgroup.||
69683|Coongan Subgroup|72668|6|Mentioned|p4|||East Pilbara Terrane.||Warrawoona Group|Includes the Duffer Formation and the Mount Ada Basalt.|Overlain by the Salgash Subgroup. Overlies the Talga Talga Subgroup.||
69683|Coongan Subgroup|73598|6|Mentioned|p1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Warrawoona Group.|Mount Ada Basalt, Duffer Formation.|Overlies Talga Talga Subgroup. Is overlain by Salgash Subgroup.||
33215|Coonieena Basalt|23415|5|Briefly described|Map Legend|Archean|Archean|Of Gorge Creek Group. Geological province: Pilbara Craton. Pillowed and massive basalt, hyaloclastic breccia, and silicified basaltic andesite; metamorphosed.||||||07-NOV-08
33215|Coonieena Basalt|23757|4|Described|p11|Archean|Archean|Of Gorge Creek Group. Disconformably overlain by Cattle Well Formation. Geological Province: Pilbara Craton. Comprises massive and pillowed, metamorphosed tholeiitic basalt.||||||07-NOV-08
33215|Coonieena Basalt|24025|4|Described|p8 Tb. 1|Archean|Archean|Of Gorge Creek Group.  Massive and pillowed tholeiitic basalt, silicified andesite with minor high-Mg basalt.  Max. thickness: 1500m.  Geological Province: Pilbara Craton.||||||07-NOV-08
33215|Coonieena Basalt|50544|5|Briefly described|p33, p21 Tb. 4|Archean|Archean|Of the Gorge Creek Gp.  Pillowed and massive tholeiitic basalt, basaltic andesite, high-Mg basalt, mafic pisolitic tuff.  Conformably overlain by Eel Creek Fm; disconformably overlies Cundaline Fm; unconformably over Nimingarra Fm.  Max. thick: ~1500m||||||07-NOV-08
33215|Coonieena Basalt|50555|5|Briefly described|Map legend|Archean|Archean|Of the Gorge Creek Group (Pilbara Supergroup).   Pillowed and massive basalt, hyaloclastic breccia and silicified basaltic andesite.  Geological Province: Pilbara Craton.||||||07-NOV-08
33215|Coonieena Basalt|63441|6|Mentioned|p29|Archean|Archean|Of Williams (1999).Of the former Gorge Creek Group. Now reassigned as Coonieena Basalt Member of Bookingarra Formation (Croydon Group) based on geochemical data.||||||07-FEB-11
33215|Coonieena Basalt|63538|5|Briefly described|p7, p8 Tb. 1, p17|Archean|Archean|Geological Province: Plibara Craton. Basalt.||||||07-FEB-11
33215|Coonieena Basalt|67201|5|Briefly described|p12 Tb.1|||Pilbara Craton, De Grey Superbasin, Mallina Basin. See Coonieena Basalt Member.||Croydon Group||||22-NOV-16
33215|Coonieena Basalt|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean||||||Massive and pillowed basalt and komatiitic basalt; local silicified basaltic andesite and hyaloclastic breccia; metamorphosed|
33215|Coonieena Basalt|69301|5|Briefly described|p9 Tb.1. p15|||Pilbara Craton. Mallina Basin.||Croydon Group||||
33215|Coonieena Basalt|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton. Of Mallina Basin, De Grey Superbasin. Events: North Pilbara Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv.|3016-2980 Ma (inferred)||||Massive and pillowed basalt and komatiitic basalt; local silicified basaltic andesite and hyaloclastic breccia; metamorphosed|
33215|Coonieena Basalt|70022|6|Mentioned|p115|||East Pilbara Terrane.||Croydon Group.||||
33215|Coonieena Basalt|70775|6|Mentioned|p54. p56|||This unit extends to the Bamboo Creek-Coppin Gap area of the east Pilbara. Name first used by Williams (1999) who assigned this to the Gorge Creek Group. Correlation with the Bookingarra Group has been precluded by geochronology. This unit is currently not assigned to a group.|c. >2990 Ma|||||
33215|Coonieena Basalt|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|De Grey Superbasin.||De Grey Supergroup|||Massive and pillowed basalt and komatiitic basalt; local silicified basaltic andesite and hyaloclastic breccia; metamorphosed.|
33215|Coonieena Basalt|72251|5|Briefly described|p54|Mesoarchean|Mesoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||||Overlain by Cattle Well Formation. Underlain unconformably bv Cundaline Formation or Farrel Quartzite.||
33215|Coonieena Basalt|73598|6|Mentioned|p1212|Mesoarchean|Mesoarchean|East Pilbara Terrane.||De Grey Supergroup.||Unconformably overlies Cundaline Formation. Is overlain by Cattle Well Formation.||
69684|Coonterunah Subgroup|61253|5|Briefly described|p51, p52 Fig. 2|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Supersedes the Coonterunah Group, now downgraded in status. Geological Province: Pilbara Craton.||||||07-NOV-08
69684|Coonterunah Subgroup|62979|5|Briefly described|p213 Fig. 1|Archean|Archean|Of the Warrawoona Group. Age: 3515 Ma. Geological Province: Pilbara Craton.||||||16-APR-13
69684|Coonterunah Subgroup|63420|5|Briefly described|Map legend|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Includes Coucal and Table Top Formations. Age: c. 3515-3498 Ma. Geological Province: Pilbara Craton.||||||16-APR-13
69684|Coonterunah Subgroup|63441|4|Described|p4 Tb. 1, p19|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Replaces Coonterunah Group.Comprises Table Top, Coucal, Double Bar and Dresser Formations.  Ages: 3515 +/- 3 Ma and 3498 +/- 2 Ma.||||||16-APR-13
69684|Coonterunah Subgroup|63538|4|Described|p3 Fig. 2, p5, p7-8, p8 Tb. 1, p11|Archean|Archean|Of Warrawoona Group. Includes Table Top, Coucal and Double Bar Formations. Age: 3525-3498 Ma. Geological Province: Pilbara Craton. Komatiite to dacite.||||||16-APR-13
69684|Coonterunah Subgroup|64405|5|Briefly described|p2 Fig. 1|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Geological province: East Pilbara Terrane.||||||07-FEB-11
69684|Coonterunah Subgroup|64580|4|Described|map legend||Paleoarchean|Mafic volcanic rocks; local felsic and ultramafic rocks; metamorphosed.||||||15-DEC-08
69684|Coonterunah Subgroup|64747|5|Briefly described|p94 fig 1, p95|Paleoarchean|Paleoarchean||c.3515-3498 Ma (Van Kranendonk et al. 2006)|Unit in Warrawoona Group.||||
69684|Coonterunah Subgroup|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Shown as combined Tabletop, Coucal and Double Bar Formations. Age shown as >3515 Ma to <3498 Ma.||||||
69684|Coonterunah Subgroup|66217|5|Briefly described|p8, p14.|Paleoarchean|Paleoarchean|Of Van Kranendonk et al. (2006a). These rocks were formerly ascribed to the Coonterunah Group. Rocks of this Subgroup not exposed in the Coongan sheet area.|3515-3490 Ma.|Basal unit in Warrawoona Group.|Includes Tabletop, Coucal and Double Bar Formations.|Is overlain by Talga Talga Subgroup.||10-JUN-20
69684|Coonterunah Subgroup|66664|6|Mentioned|p3.  |||East Pilbara Terrane||Unit in Warrawoona Group.||Underlies Talga Talga Subgroup.||
69684|Coonterunah Subgroup|66745|6|Mentioned|p57.|Paleoarchean|Paleoarchean|||Unit in Warrawoona Group.|Includes Table Top, Coucal and Double Bar Formations.|||
69684|Coonterunah Subgroup|67197|4|Described|p2-5, p7-12, p14-31, p33-34, p36-38, p40|Paleoarchean|Paleoarchean|See also p52, p55-56, p62-63. Pilbara Craton. Interpreted as a separate Group in the Pilbara Supergroup by Van Kranendonk et al. (2002). Photographs of outcrops. Black chert dykes intruding Strelley Pool Formation originate from this unit.|3525-3490 Ma.|Warrawoona Group.|Table Top, Coucal, Double Bar Formations.|Is overlain by Talga Talga Subgroup; locally overlain unconformably by Strelley Pool Formation.|Includes metavolcanic rocks, grey/green tuff, chert and BIF.|
69684|Coonterunah Subgroup|67201|4|Described|p7 Fig.4|||In northern Pilbara Craton, East Pilbara Terrane.||Warrawoona Group|Double Bar Formation, Coucal Formation, Table Top Formation|||
69684|Coonterunah Subgroup|67269|5|Briefly described|p6 Fig.3|Paleoarchean|Paleoarchean|||Warrawoona Group.|Table Top, Coucal, Double Bar Formations.|||
69684|Coonterunah Subgroup|67270|5|Briefly described|p3-4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Warrawoona Group.|Table Top, Coucal, Double Bar Formations.|Is overlain by Talga Talga Subgroup.||
69684|Coonterunah Subgroup|68035|5|Briefly described|p288 Fig 4|||Pilbara Supergroup, East Pilbara Terrane.||Of Warrawoona Group. |Includes Table Top Formation, Coucal Formation, Double Bar Formation.|||
69684|Coonterunah Subgroup|68280|6|Mentioned|p4, p13, p19||||c. 3515 Ma|Warrawoona Group|Includes Double Bar Formation, Coucal Formation, Table Top Formation|||13-JAN-23
69684|Coonterunah Subgroup|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Warrawoona Group.|Includes Double Bar Formation, Coucal Formation, Table Top Formation.|||23-SEP-13
69684|Coonterunah Subgroup|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c.3515-3498 Ma (Buick et al. 1995).|Of the Warrawoona Group.|Includes Coucal Formation, Table Top Formation.|||06-JAN-15
69684|Coonterunah Subgroup|68284|5|Briefly described|p7|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Warrawoona Group.|Table Top, Coucal, Double Bar Formations.|||
69684|Coonterunah Subgroup|69013|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Of the Warrawoona Group.|Includes the Coucal Formation and the Table Top Formation.||Includes amphibolite and mafic schist; ferruginous chert; basalt and andesite; amphibolite; metadolerite; banded iron-formation and interleaved mafic or ultramafic schist.|30-APR-14
69684|Coonterunah Subgroup|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. ||Of the Warrawoona Group.|Includes Double Bar Formation, Coucal Formation, and Table Top Formation.|||
69684|Coonterunah Subgroup|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Age derived from sample of quartzite (168993.1.pdf) and is the age of volcanigenic component of the sandstone protolith.|3508 Ma +/- 3 Ma (SHRIMP)|Warrawoona Group|Includes Coucal Formation, Table Top Formation, Double Bar Formation||Mafic volcanic rocks; metamorphosed|
69684|Coonterunah Subgroup|69185|4|Described|GEOL_LUT_CSV files||Paleoarchean|Geological province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 3615 Ma|Unit of Warrawoona Group.|||Felsic and mafic volcanic rocks; local ultramafic rocks; metamorphosed|
69684|Coonterunah Subgroup|69301|5|Briefly described|p5 Fig.3, p11|||Pilbara Craton. East Pilbara Terrane.||Warrawoona Group|Double Bar Formation, Coucal Formation, Table Top Formation|||
69684|Coonterunah Subgroup|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA 168993 (volcaniclastic sandstone) yielded an intepreted igneous crystallisation age of 3508+\-3 Ma for the volcanigenic components of the sandstone (weghted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|3515-3490 Ma (inferred)|Unit of Warrawoona Group.|Includes Coucal Formation, Double Bar Formation.||Mafic volcanic rocks; metamorphosed|
69684|Coonterunah Subgroup|69989|6|Mentioned|p26|Paleoarchean|Paleoarchean|North Pole Dome area, Pilbara Craton.|3.51 Ga.|Warrawoona Group.||Is overlain by Dresser Formation.||
69684|Coonterunah Subgroup|70022|5|Briefly described|p113, 115, 121|||East Pilbara Terrane. Another age determination is 3498 +/- 2 Ma by Nelson (2002).|3515 +/- 3 Ma (Pb/Pb; Buick et al., 1995).|Warrawoona Group.|Table Top, Coucal, Double Bar Formations.|Is overlain by the Dresser Formation.|Includes volcaniclastic sandstones.|
69684|Coonterunah Subgroup|70729|6|Mentioned|p164|||Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawoona Group.||||
69684|Coonterunah Subgroup|70733|6|Mentioned|p105|||Eastern Pilbara Craton.||Warrawoona Group.||||
69684|Coonterunah Subgroup|70775|5|Briefly described|p2|Paleoarchean|Paleoarchean|These are some of the oldest exposed rocks in the Pilbara Craton.|c. 3530-3490 Ma|Warrawoona Group||||
69684|Coonterunah Subgroup|70884|5|Briefly described|p123|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawoona Group.|Incldues Double Bar, Coucal and Table Top formations.|Overlain by Talga Talga Subgroup/North Star Basalt. Underlain by .||
69684|Coonterunah Subgroup|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||basalt, komatiitic (high-mg) basalt, banded inronformation, greenschist facies rocks|
69684|Coonterunah Subgroup|71487|5|Briefly described|p128|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawonna Group.||Lowermost unit of Warrawoona Group. Overlain by Talga Talga Subgroup.||
69684|Coonterunah Subgroup|72034|6|Mentioned|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Double Bar Formation, Coucal Formation, Table Top Formation.|||
69684|Coonterunah Subgroup|72251|5|Briefly described|p54|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawonna Group.|includes Double Bar, Coucal and Table Top formations.|Lowermost unit of Warrawoona Group. Overlain by Talga Talga Subgroup.||
69684|Coonterunah Subgroup|72668|5|Briefly described|p4-5, p8, p10, p17, p25, p27|||North-western part of the East Pilbara Terrane.|c. 3520-3490 Ma|Warrawoona Group|Includes the Table Top Formation, the Coucal Formation and the Double Bar Formation.|Overlain by the Talga Talga Subgroup. Unconformably overlain by the Kelly Group.||13-JAN-22
69684|Coonterunah Subgroup|73598|6|Mentioned|p1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Warrawoona Group.|Table Top, Coucal, Double Bar Formations.|Is overlain by Talga Talga Subgroup.||
38575|Coor-de-wandy Formation|23781|5|Briefly described|p5|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
38575|Coor-de-wandy Formation|24544|4|Described|p3|Paleoproterozoic|Paleoproterozoic|Age: >1800 Ma. Siliclastic micaceous metasediments. Unconformably overlain by Mount James Formation.||||||07-NOV-08
38575|Coor-de-wandy Formation|50218|5|Briefly described|p241 Fig. 3|||Metasedimentary rocks. Geological Province: Errabiddy Shear Zone.||||||07-FEB-11
38575|Coor-de-wandy Formation|50220|5|Briefly described|p281 Fig.1|||||||||
38575|Coor-de-wandy Formation|63866|5|Briefly described|p155, p157-p159, p168|Paleoproterozoic|Paleoproterozoic|||||Unconformably overlain by the Mount James Formation.||
38575|Coor-de-wandy Formation|64580|4|Described|map legend||Paleoproterozoic|Siliciclastic sedimentary rocks; metamorphosed.||||||15-DEC-08
38575|Coor-de-wandy Formation|69003|6|Mentioned|p4, p33|Paleoproterozoic|Paleoproterozoic|Gascoyne Province, Capricorn Orogen.||Pooranoo Metamorphics.||||
38575|Coor-de-wandy Formation|69028|5|Briefly described|Map Legend|Statherian|Orosirian|Gascoyne Province.||Of the Pooranoo Metamorphics.|||Siliciclastic sedimentary rock; metamorphosed.|06-MAY-14
38575|Coor-de-wandy Formation|69166|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Siliciclastic sedimentary rocks; metamorphosed.|
38575|Coor-de-wandy Formation|69583|5|Briefly described|p130, Plate 3.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|||||Metamorphosed siliciclastic sedimentary rock.|
38575|Coor-de-wandy Formation|70795|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|West Australian Craton|2500-1600 Ma||||Siliciclastic sedimentary rock; metamorphosed.|
38575|Coor-de-wandy Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||metasedimentary rock|
38575|Coor-de-wandy Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Gascoyne Province, Capricorn Orogen.|||||Siliciclastic sedimentary rock; metamorphosed.|
38575|Coor-de-wandy Formation|72259|6|Mentioned|p3, App. Tb.B|Statherian|Statherian|[Misseplt as Coor-de-Wandy Formation on p3].|ca. 1800-1600 Ma|||||
26299|Coorong Creek Adamellite|39444|2|Defined|Table 3|Archean|Archean|||||||07-NOV-08
26299|Coorong Creek Adamellite|39697|3|Fully described|p39|||||||||
26299|Coorong Creek Adamellite|44150|5|Briefly described|p144 Tb.2-21, p149 Fig.2-137|||110 sq. km.||Yule Granitoid Complex|||Biotite monzogranite, foliated in the north Pilbara.|
75915|Cootharra Monzogranite|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane||Walganna Suite|||Medium- to coarse-grained monzogranite; muscovite monzogranite; medium- to coarse-grained; undeformed.|
75915|Cootharra Monzogranite|69014|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Murchison Domain. Age constrained by the Walganna Suite.||Of the Walganna Suite.|||Medium- to coarse-grained monzogranite; undeformed.|01-MAY-14
75915|Cootharra Monzogranite|69628|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton||Walganna Suite|||Medium- to coarse-grained monzogranite, undeformed; muscovite monzogranite, medium- to coarse-grained, undeformed.|
75915|Cootharra Monzogranite|70139|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton.||Walganna Suite.|||Undeformed, medium- to coarse-grained monzogranite.|
75915|Cootharra Monzogranite|70796|5|Briefly described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton. See also 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, Reedy100_2543_stratig.pdf, Wynyangoo100_2542_stratig.pdf.|ca 2647 to 2600 Ma (inferred)|Walganna Suite|||Medium to coarsegrained monzogranite; undeformed. Muscovite monzogranite; medium to coarse grained; undeformed.|
75915|Cootharra Monzogranite|71159|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton. The four facies are mapped separately.||Walganna Suite.|||Medium- to coarse-grained monzogranite, undeformed; medium- to coarse-grained muscovite monzogranite, undeformed.|
75915|Cootharra Monzogranite|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.|2650-2600 Ma (inferred)|Unit of Walganna Suite.|||Medium- to coarse-grained monzogranite; undeformed, muscovite monzogranite; medium to coarse grained; undeformed.|
81574|Copernicus pyroxenite|71873|5|Briefly described|p425,431-434,437-441,443-444|Orosirian|Orosirian|Geological province: Lamboo Province. Ni-Cu mineralized unit; has contaminated, arc-like geochemistry, occurring synchronous with the Halls Creek Orogen and intrusion of the Sally Downs Supersuite. See also Copernicus Intrusion, intrusion.|1823+/-3  Ma U-Pb SHRIMP crystallisation age.|||||03-SEP-19
37086|Copper Chert|23723|6|Mentioned|p53|||Geological Province: Bangemall Basin.||||||
40472|Copperfield Monzogranite|50075|5|Briefly described|p16|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
40472|Copperfield Monzogranite|50076|5|Briefly described|Map|Archean|Archean|Biotite monzogranite with prominent mineral lineation.  Geological Province: Yilgarn Craton.||||||07-NOV-08
40472|Copperfield Monzogranite|50318|5|Briefly described|Map legend|Archean|Archean|Biotite monzogranite with prominent mineral lineation.||||||07-NOV-08
40472|Copperfield Monzogranite|64771|5|Briefly described|p16-17|||Crops out in the core of the Kurrajong Anticline, West Ida greenstone belt. No geochronology due to lack of zircons. Numerous gold deposits (eg Baldock) in greenstones at the margins of this unit.|||||Weakly foliated monzogranite with well-developed, pervasive stretching lineation.|
40472|Copperfield Monzogranite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Biotite monzogranite with prominent mineral lineation.||||||07-FEB-11
40472|Copperfield Monzogranite|68289|5|Briefly described|p21-p22|||Outcrops in the core of the Kurrajong anticline within the Mount Ida greenstone belt.||||||
40472|Copperfield Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Meta biotite monzogranite with prominent mineral lineation.|05-AUG-15
40472|Copperfield Monzogranite|69631|5|Briefly described|p33, p35-36|||Crops out in the core of the Kurrajong Anticline, within the Mount Ida greenstone belt. Several attempts to date this unit have failed for lack of zircons. Numerous gold deposits have been historic producers from greenstones at the margins of this unit.|||||Medium- to coarse-grained; quartz-plagioclase-microcline, with biotite the predominant mafic mineral, and minor magnetite and apatite. Has a weakly-developed foliation, and a very well-developed, pervasive stretching lineation.|
40472|Copperfield Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|See also 500k_interpgeop14_lut.csv.|3010 - 2600 Ma (inferred).||||Biotite metamonzogranite with prominent mineral lineation.|
40472|Copperfield Monzogranite|70773|6|Mentioned|p49|||||||||
40472|Copperfield Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv.|3010-2600 Ma (inferred)||||Meta biotite monzogranite with prominent mineral lineation|
40472|Copperfield Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Mesoarchean|Yilgarn Craton.|||||Biotite metamonzogranite with prominent mineral lineation.|
78620|Copperhead Igneous Complex|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Data from OZCHRON1. Comment for Copperhead carbonatite: 'The ages of the zircon suites are complex, with 1821 Ma being the interpreted magmatic age from 28 analyses. A lower Th/U group is older (1840-1880 Ma) and late Archaean xenocryst cores are 2419-2736 Ma.'|Interp magmatic age 1821+/-4 Ma U/Pb SHRIMP||||Albitite, albite-carbonate fenite, carbonate veins, and carbonatite breccia.|30-JUL-15
78620|Copperhead Igneous Complex|70154|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1821 Ma||||Albitite, albite-carbonate fenite, carbonate veins and carbonatite breccia.|
33873|Coppermine Shale|22534|6|Mentioned|Fig.8 p18|||||||||
33873|Coppermine Shale|50551|5|Briefly described|p1094 Fig.5||Archean|In Eastern Goldfields Province.||||||07-NOV-08
33873|Coppermine Shale|65834|6|Mentioned|p39|||Mount Pleasant district, Ora Banda Domain, Kalgoorlie Terrane.||||Is overlain by Bent Tree Basalt.||
33873|Coppermine Shale|73391|5|Briefly described|p51, 329|||Mount Pleasant Anticline. An interflow unit.||||Overlies Mount Pleasant Sill. Is overlain by Bent Tree Basalt.||
36951|Coppin Gap Granodiorite|23585|6|Mentioned|p13|||||||||
36951|Coppin Gap Granodiorite|23783|5|Briefly described|p83|Archean|Archean|Age: 3314+/-13Ma.||||||07-NOV-08
36951|Coppin Gap Granodiorite|24110|5|Briefly described|Plate 1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
36951|Coppin Gap Granodiorite|24185|5|Briefly described|p739 Tb.3|Archean|Archean|Age: 3314 +/- 3 Ma (SHRIMP zircon U-Pb, Thorpe et al, 1992). Geological Province: Pilbara Craton.||||||07-NOV-08
36951|Coppin Gap Granodiorite|44229|5|Briefly described|Map legend|Archean|Archean|Part of the Mount Edgar Granitoid Complex.  Massive to seriate, cream to pinkish, biotite granodiorite, and tonalite; weakly foliated.||||||07-NOV-08
36951|Coppin Gap Granodiorite|50189|4|Described|p15, 22|Archean|Archean|Of the Mount Edgar Granitoid Complex. Massive to seriate, pink and grey, medium-grained granodiorite, more felsic in north due to increased quartz and K-feldspar. Age: c.3314Ma. Intrudes the Mount Ada Basalt.||||||07-NOV-08
36951|Coppin Gap Granodiorite|50544|5|Briefly described|p30-31, p19 Tb. 2 (amended)|Archean|Archean|Of the Mount Edgar Granitoid Complex.  Constitutes the main part of the complex on YARRIE.   Age: 3314+/-13Ma (Williams and Collins, 1990).  Intrudes Mount Ada and Apex Basalts.||||||07-NOV-08
36951|Coppin Gap Granodiorite|50555|5|Briefly described|Map legend|Archean|Archean|Of the Mount Edgar Graniotid Complex. Massive to seriate, cream to pinkish biotite granodiorite and tonalite.  Age: c.3314Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
36951|Coppin Gap Granodiorite|60429|5|Briefly described|p6 Fig. 3, p7|Archean|Archean|Main component of Mount Edgar Granitoid Complex on MUCCAN. Age: c.3314Ma. Geological Province: Pilbara Craton. Contains massive to seriate, pink and grey, medium-grained granodiorite; more felsic to the north.||||||07-FEB-11
36951|Coppin Gap Granodiorite|63417|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite.  Age: 3314Ma. Geological Province: Pilbara Craton. Biotite granodiorite and tonalite; medium-grained, massive to seriate, weakly foliated; local mafic xenoliths, metamorphosed.||||||07-NOV-08
36951|Coppin Gap Granodiorite|63420|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite. Age: c.3314Ma. Geological Province: Pilbara Craton. Massive to foliated, cream to pinkish biotite granodiorite to tonalite; weakly foliated.||||||07-NOV-08
36951|Coppin Gap Granodiorite|63441|5|Briefly described|p8 Tb. 2|Archean|Archean|Of Emu Pool Supersuite. Replaces Coppin Gap Suite. Age: 3314+/-13Ma. Geological province: Pilbara Craton.||||||07-FEB-11
36951|Coppin Gap Granodiorite|64405|6|Mentioned|p14|Archean|Archean|Of Williams and Collins (1990). Age: 3314+/-3Ma.||||||07-FEB-11
36951|Coppin Gap Granodiorite|64580|4|Described|map legend||Paleoarchean|Of Emu Pool Supersuite. Biotite granodiorite and tonalite; medium grained, massive to seriate, weakly foliated; local mafic xenoliths; weakly metamorphosed.||||||22-OCT-08
36951|Coppin Gap Granodiorite|64936|5|Briefly described|map legend|Archean|Archean|Of Mount Edgar Granitoid Complex. Age: c. 3314 Ma (geochronology: IS Williams and WJ Collins 1990). Biotite granodiorite to tonalite. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
36951|Coppin Gap Granodiorite|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.|c.3314 Ma (Wyatt et al. 2001).|Of Mount Edgar Granitoid Complex.|||Biotite granodiorite and tonalite, massive to seriate, cream to pinkish, weakly foliated; granitoid rock with mafic and ultramafic xenoliths.|
36951|Coppin Gap Granodiorite|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c.3314 Ma (Williams and Collins 1990).|Of Emu Pool Supersuite.|||Biotite granodiorite and tonalite, medium-grained, massive to seriate, weakly foliated, local mafic xenoliths; granitic rock with mafic and ultramafic xenoliths; weakly metamorphosed.|
36951|Coppin Gap Granodiorite|65827|3|Fully described|p6 Tb.2, p9 Fig 3, p17, p24-25, p57|Paleoarchean|Paleoarchean|Williams (1999); originally in Coppin Gap Suite (Collins 1983). Of Emu Pool Supersuite. 3314 +/- 13 Ma SHRIMP U-Pb zircon (Williams and Collins 1990). Intruded by Bishop Creek Monzogranite, Munganbrina Monzogranite, Mullugunya Granodiorite; intrudes Mount Ada Basalt; contains numerous xenoliths probably from Mount Ada Basalt; originally included in Coppin Gap Suite. Weakly foliated, medium-grained granodiorite and tonalite.||||||
36951|Coppin Gap Granodiorite|66217|4|Described|p5, pp32-33.|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Formerly Coppin Gap Suite (Collins 1983; Williams and Collins 1990). Age from U-Pb SHRIMP zircon. Source of significant Cu-Mo mineralisation.|3314 +/- 13 Ma (Williams and Collins 1990).|Unit in Emu Pool Supersuite.||Intrudes Coongan Subgroup (Pilbara Supergroup). Is intruded by Munganbrina Monzogranite and Cleland Supersuite.|Non-foliated to weakly foliated, pink and cream, granodiorite and tonalite; medium-grained, equigranular to seriate-textured.|
36951|Coppin Gap Granodiorite|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c.3314 Ma (Williams and Collins, 1990).|Of the Emu Pool Supersuite.|||Massive to foliated, cream to pinkish biotite granodiorite to tonalite; weakly foliated.|
36951|Coppin Gap Granodiorite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Emu Pool Supersuite||Intruded by Bridget Suite|Biotite granodiorite and tonalite, granitic rock with mafic and ultramafic xenoliths; weakly metamorphosed. Porphyritic microgranodiorite and micromonzogranite; metamorphosed.|
36951|Coppin Gap Granodiorite|69185|4|Described|500k_geologyp08_lut.csv||Paleoarchean|Geological Province: Pilbara Craton.||Unit of Emu Pool Supersuite.|||Biotite granodiorite and tonalite; medium grained, massive to seriate, weakly foliated; local mafic xenoliths; weakly metamorphosed|
36951|Coppin Gap Granodiorite|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA 142825 (granodiorite) yielded an interpreted minimum igneous crystallisation age of 1730+\-9 Ma (40Ar-30Ar). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|3317-3314 Ma (isotopic)|Unit of Emu Pool Supersuite.||Intrudes into Bridget Suite.|Porphyritic microgranodiorite and micromonzogranite; metamorphosed; biotite granodiorite and tonalite, metamorphosed; granotic rock with mafic and ultramafic xenoliths, weakly metamorphosed.|
36951|Coppin Gap Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite, tonalite|
36951|Coppin Gap Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||Max age 3317+/-3 Ma, min 3314+/-13 Ma.|Emu Pool Supersuite|||Biotite granodiorite and tonalite; medium grained, massive to seriate, weakly foliated; local mafic xenoliths; weakly metamorphosed.|
30536|Coramup Gneiss|22448|6|Mentioned|p877 Fig.3||Ectasian|||||||
30536|Coramup Gneiss|22792|6|Mentioned|p57|||||||||
30536|Coramup Gneiss|24165|5|Briefly described|Plate 1|Mesoproterozoic|Mesoproterozoic|||Biranup Complex.|||Heterogeneous granitoid gneiss, mainly derived from Recherche Granite, deformed with orthogneiss and paragneiss.|
30536|Coramup Gneiss|43203|5|Briefly described|Map Legend||Proterozoic|Biranup Complex||||||
30536|Coramup Gneiss|43212|6|Mentioned|p7|||U-Pb SHRIMP of this complex formed at c.1300 Ma.||||||
30536|Coramup Gneiss|43498|4|Described|4||Proterozoic|U-Pb ages: 1600-1700Ma.||||||16-JAN-14
30536|Coramup Gneiss|62381|5|Briefly described|p2 Fig.2.|||A 10 km wide ductile shear zone between the Coramup and Bremer faults. Protoliths include Dalyup Gneiss and 1300-1280 Ma granite.||||||01-JUL-14
30536|Coramup Gneiss|63866|4|Described|p183, p185, p188-p189, p191, p198|Statherian|Statherian|Biranup Complex. Metamorphosed at 1231 +/- 9 Ma (Spaggiari et al, 2007). The metamorphosed quartz sandstone has a maximum U-Pb depositional age of c. 1750 Ma and was metamorphosed at 1215 +/- 5 Ma.|1688 +/- 12 Ma (SHRIMP U-Pb)||||Garnet-bearing granodioritic gneiss and metamorphosed quartz sandstone.|
30536|Coramup Gneiss|64577|5|Briefly described|p606 Fig. 1, p616, p617|||Of Biranup Complex. Age: 1700-1630Ma.||||||
30536|Coramup Gneiss|64580|4|Described|map legend|Mesoproterozoic|Paleoproterozoic|Granitic gneiss; heterogeneous; mainly derived from Recherche Granite; deformed with orthogneiss (c. 1700-1600 Ma) and paragneiss; including quartzite (?c. 1550 Ma).||||||15-DEC-08
30536|Coramup Gneiss|65487|3|Fully described|p37,41-43, 2-3,24-29,50-60; Figs.1-2,27|||Part of the Biranup Zone (Kepa Kurl Booya Province); Albany-Fraser Orogen. Interpreted as an exotic terrane dominated by granitic rocks with protoliths 1690-1660 Ma and reworked gneissic equivalents; a 10-20km wide belt of intensely deformed heterogeneous gneisses. Distinctly linear magnetic character. Deformation and geochronology described in detail. Includes finely layered granitic to granodioritic gneiss, tonalitic gneiss, lenses and boudins of metamafic rocks, quartz-rich psammite, minor migmatitic metapelite, and rare thin boudins of calc-silicate rocks.||||||16-JAN-14
30536|Coramup Gneiss|67268|5|Briefly described|p4, p6, p7, p14, p15, p16, p19|Paleoproterozoic|Paleoproterozoic|Similar to the Dalyup Gneiss in age and lithology. Metamorphism of this unit coincided with the emplacement of the Recherche Supersuite. Shown as Coramup Hill Orthogneiss p10.|1690-1660 Ma (Bodorkos & Clark 2004)|||Intruded by the Recherche Supersuite, Esperance Supersuite|Layered granitic to granodioritic gneisses,  tonalite gneiss, paragneiss, orthogneiss, minor mafics, psammitic migmatitic metapelite and minor calc-silicates.|15-JUN-22
30536|Coramup Gneiss|67722|5|Briefly described|p5 fig 2.2, p8-10, p16, p17, p97|Paleoproterozoic|Paleoproterozoic|Biranup Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen. Consists of older metasedimentary and metagranitic rocks with ages comparable to other Biranup Zone rocks. |1700-1650 Ma(SHRIMP)|||Intruded by Recherche Supersuite|Orthogneiss and paragneiss, metagranitic rocks.|
30536|Coramup Gneiss|68186|6|Mentioned|p8, p19|||Biranup Zone, Kepa Kurl Booya Province.||||||
30536|Coramup Gneiss|68654|5|Briefly described|p20|Mesoproterozoic|Mesoproterozoic|Coramup Shear Zone, Biranup Zone, Barren Basin.|~1300 Ma||||Metasedimentary rocks.|
30536|Coramup Gneiss|69152|5|Briefly described|500k_geologyp08_lut|Mesoproterozoic|Paleoproterozoic||||||Granitic gneiss; heterogeneous; mainly derived from Recherche Granite; deformed with orthogneiss (c. 1700-1600 Ma) and paragneiss; including quartzite (?c. 1550 Ma).|05-AUG-15
30536|Coramup Gneiss|69252|5|Briefly described|p13-14|||Biranup Zone (formerly the Biranup Complex), Kepa Kurl Booya Province.|||||Orthogneisses and metagabbros. Includes paragneisses.|
30536|Coramup Gneiss|69595|5|Briefly described|p10 tbl 2, p15, p17 tbl 3, p18, p19,|Statherian|Statherian|Eastern Biranup Zone, Barren Basin. May have been deposited in a deep marine setting. Other significant age components given [see page 18]. Significant portions of this unit are made up of c. 1800 Ma detritus. See also  p32 fig 17, p33, p34 fig 19, p35, p38, p57.|1757 +/- 39 - 1688 +/- 12 Ma ||||Interbedded sandstone, mudstone and elsewhere psammitic gneiss.|
30536|Coramup Gneiss|70085|6|Mentioned|p234 Fig.1|||Biranup Zone, Albany-Fraser Orogeny.||||||
30536|Coramup Gneiss|70090|4|Described|p444,446-447,449,451-453,457-458|Statherian|Statherian|Geological province: Fraser Zone, Albany-Fraser Orogen, West Australian Craton. Depositional environment: deep marine? Associated with mafic magmatism during Biranup Orogeny. Sedimentary protoliths deposited between 1710 Ma and 1650 Ma during Biranup Orogeny. Metamorphosed to amphibolite to granulite facies. Maximum depositional age: c.2031 Ma. Minimum depositional age: contrained by c. 1688+\-12 Ma intrusive granite. Archean detrital zircon age components include c. 2650, 2623  and 2532 Ma. Paleoproterozoic age components include c. 2469, 2357, 2263, 2031, 1757 Ma.|||||Interbedded sandstone and mudstone.|
30536|Coramup Gneiss|70182|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|Deposition was coincident with the Biranup Orogeny.|1710-1650 Ma (precursors).|||||
30536|Coramup Gneiss|70732|6|Mentioned|p286|||Geological province: Biranup Zone, Albany-Fraser Orogen. Of Barren Basin. |<1688 Ma|||||
30536|Coramup Gneiss|70802|5|Briefly described|184122.1.pdf|||Geological province: Biranup Complex, Albany-Fraser Orogen. Sample GSWA 184122 (metamorphosed quartz sandstone) yielded a weighted mean 207Pb/206Pb age of 1757+\-39 Ma, interpreted as age of metamorphic zircon rim growth. Sample GSWA 184123 (gt monzogranitic gneiss) yielded a 207Pb*/206Pb* date 1688+\-12Ma, interpreted as aigneous crystallisation age of the monzogranitic precursor of the garnet-bearing gneiss.||||||
30536|Coramup Gneiss|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||felsic gneiss|
30536|Coramup Gneiss|71270|5|Briefly described|1m_geologyp12_lut.csv|||Geological province: Yilgarn Craton, West Australian Craton. |||||Granitic gneiss; heterogeneous; mainly derived from Recherche Granite; deformed with orthogneiss (circa 1700-1600 Ma) and paragneiss; including quartzite (?circa 1550 Ma)|
30536|Coramup Gneiss|73084|6|Mentioned|p12|||Albany-Fraser Orogen, Kepa Kurl Booya Province, Biranup Zone.||||||
28476|Corboy Formation|22615|6|Mentioned|p 5|||||||||
28476|Corboy Formation|22642|5|Briefly described|485|||Geol province Pilbara Craton||||||
28476|Corboy Formation|22715|5|Briefly described|table7 p214|Archean|Archean|Age: 3270-3200Ma||||||07-NOV-08
28476|Corboy Formation|22727|6|Mentioned|p638||Archean|||||||07-NOV-08
28476|Corboy Formation|23255|6|Mentioned|Fig.2|||||||||
28476|Corboy Formation|23416|5|Briefly described|Map Legend|Archean|Archean|Of Soanesville Subgroup, Pilbara Craton||||||07-NOV-08
28476|Corboy Formation|23755|4|Described|p43|Archean|Archean|See also page 17 table 1.  Of Gorge Creek Group.||||||07-NOV-08
28476|Corboy Formation|23783|5|Briefly described|p10 Fig. 5|Archean|Archean|Of Gorge Creek Group.||||||07-NOV-08
28476|Corboy Formation|24025|4|Described|p8 Tb. 1|Archean|Archean|Of Soanesville Subgroup (Gorge Creek Group). Banded iron formation, ferruginous clastic sedimentary rocks, quartzite, felsic volcanic rocks.  Max. thickness: 1000m.  Geological Province: Pilbara Craton.||||||07-NOV-08
28476|Corboy Formation|24184|6|Mentioned|p699 Fig.3|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
28476|Corboy Formation|24531|4|Described|p20|Archean|Archean|Of the Soanesville Subgroup (Gorge Creek Group).  Max. thickness: 1000m.  See also p5 Table 1.  Geological Province: Pilbara Craton.||||||07-NOV-08
28476|Corboy Formation|24532|5|Briefly described|Map legend|Archean|Archean|Of Soanesville Subgroup (Gorge Creek Group).||||||07-NOV-08
28476|Corboy Formation|24550|5|Briefly described|p31 Tb. 3.1|||Of the Gorge Creek Group. Sandstone, mudstone, conglomerate. Geological Province: Pilbara Craton.||||||07-FEB-11
28476|Corboy Formation|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Of the Soanesville Subgroup (Gorge Creek Group). Sandstone, mudstone, minor comglomerate Fe-shale, BIF, interbedded snadstone, felsic volcanic rocks.||||||07-FEB-11
28476|Corboy Formation|31853|2|Defined|p62|Archean|Archean|||||||07-NOV-08
28476|Corboy Formation|37373|4|Described|p79|||||||||
28476|Corboy Formation|38498|5|Briefly described|Table 1|||||||||
28476|Corboy Formation|38544|6|Mentioned|Fig.1|||||||||
28476|Corboy Formation|39426|6|Mentioned|p3|||See also Table 1||||||
28476|Corboy Formation|39444|6|Mentioned|Table 1|||||||||
28476|Corboy Formation|39697|4|Described|p99|||||||||
28476|Corboy Formation|41073|6|Mentioned|p200|||||||||
28476|Corboy Formation|41252|6|Mentioned|p51|||||||||
28476|Corboy Formation|41353|4|Described|p70|||||||||
28476|Corboy Formation|41354|6|Mentioned|p92|||||||||
28476|Corboy Formation|41635|6|Mentioned|Table 2|||||||||
28476|Corboy Formation|42231|5|Briefly described|p333|||||||||
28476|Corboy Formation|43698|6|Mentioned|p26|||||||||
28476|Corboy Formation|43779|5|Briefly described|p7|||||||||
28476|Corboy Formation|44150|5|Briefly described|p129 Tb.2-15, p132 Fig.2-131, p134-135|||See also p152 Tb.2-22. Absent from West Pilbara.||Soanesville Subgroup||Is overlain conformably by Charteris Basalt.|In some areas, psammitic and pelitic rocks and ferruginous metasediments; elsewhere, siltstone, cross-bedded sandstone, and quartzite.|
28476|Corboy Formation|50302|5|Briefly described|Map Legend|Archean|Archean|Of the Gorge Creek Group.  Overlies: Euro Basalt. Underlies: Nimingarra Iron Formation. Geological Province: Pilbara Craton.||||||07-NOV-08
28476|Corboy Formation|50379|5|Briefly described|Map Legend|Archean|Archean|Of Gorge Creek Group (Pilbara Supergroup). Geological Province: Pilbara Craton.||||||07-NOV-08
28476|Corboy Formation|50383|5|Briefly described|Map Legend|Archean|Archean|Of Gorge Creek Group (Pilbara Supergroup). Geological Province: Pilbara Craton||||||07-NOV-08
28476|Corboy Formation|61253|5|Briefly described|p51|Archean|Archean|Of the Gorge Creek Group.  Geological Province: Pilbara Craton.||||||07-NOV-08
28476|Corboy Formation|61266|4|Described|p58 Tb.1, p60|Archean|Archean|Of Soanesville Subgroup. Overlies mafic volcanic rocks of the Sulphur Springs Group or Warrawoona Group. In places conformably overlies Pincunah Hill Formation. Intruded by Dalton Suite. Sandstone, mudstone, minor conglomerate. Geol. Prov: Pilbara Craton||||||07-NOV-08
28476|Corboy Formation|61579|5|Briefly described|p58 Fig. 2|Archean|Archean|Of the Gorge Creek Group.||||||07-NOV-08
28476|Corboy Formation|63441|5|Briefly described|p4 Tb. 1|Archean|Archean|Of the Soanesville Group (Pilbara Supergroup).||||||07-FEB-11
28476|Corboy Formation|63538|5|Briefly described|p6 Fig. 3|Archaean|Archaean|Of Soanesville Group. Underlain by Pincunah Hill Formation, overlain by Paddy Market Formation. Geological Province: Pilbara Craton. Sedimentary rocks.||||||15-AUG-18
28476|Corboy Formation|64328|5|Briefly described|p56 Tb. 1|||Of the Soanesville Subgroup (Gorge Creek Group).||||||07-FEB-11
28476|Corboy Formation|64384|5|Briefly described|p26 Tb. 3|Archean|Archean|Of the Gorge Creek Group. Max. thickness: 2km.||||||07-FEB-11
28476|Corboy Formation|64405|5|Briefly described|p4 Fig. 3|Archean|Archean|Name inferred from Corboy only in Figure 3. Of the Soanesville Group (De Grey Supergroup). Sedimentary.||||||07-FEB-11
28476|Corboy Formation|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of George Creek Group. Geological Province: Pilbara Craton. Quartz sandstone, fuchsitic quartz sandstone, banded chert, sandstone, basal cobble to pebble polymictic conglomerate; weakly metamorphosed.||||||07-FEB-11
28476|Corboy Formation|64936|5|Briefly described|map legend|Archean|Archean|Of Soanesville Subgroup. Under Paddy Market Formation; over North Star Basalt. Conglomerate; sandstone and siltstone; quartz arenite. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
28476|Corboy Formation|65008|4|Described|p7, p8 Fig.5, p14, p28, p41|Mesoarchean|Paleoarchean|East Pilbara Granite-Greenstone Terrane. Basal unit of the Gorge Creek Group. Sandstone: cross-laminated with graded bedding. Conglomerate: matrix supported with metasandstone clasts, coloured and banded chert, and white vein quartz.|3235-2950 Ma|Of the Gorge Creek Group||Unconformably underlain by the  Charteris Basalt, Wyman and Budjan Creek Formations. Overlain by the Mount Roe Basalt and Hardey Formation (unconformably), and Paddy Market Formation (conformably).|Consists of sandstone with a lensoidal basal polymictic conglomerate and is interbedded with banded and ferruginous chert, black carbonaceous shale, and siltstone.|
28476|Corboy Formation|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||Of Gorge Creek Group.||Is overlain by Nimingarra Iron Formation.|Quartzite, fuchsitic quartzite, and weakly metamorphosed banded chert, sandstone and polymictic conglomerate; chert and banded chert, weakly metamorphosed.|
28476|Corboy Formation|65827|6|Mentioned|Tb.1 p6|Paleoarchean|Paleoarchean|Name used on original map (2004), not included on revised map. Formerly of Gorge Creek Group. Unconformably overlies Budjan Creek Formation; underlies Nimingarra Iron Formation?||||||
28476|Corboy Formation|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Unit in Soanesville Group. Age shown as c.3190 Ma. Metamorphosed siliciclastic sedimentary rocks.||||||
28476|Corboy Formation|66118|5|Briefly described|p149 Fig.3|||Pilbara Craton. East Pilbara Terrane. ||||Dalton Suite intrudes Corboy Formation in Soanesville greenstone belt. Is overlain by Paddy Market Formation. Overlies Pincunah Hill Formation.||
28476|Corboy Formation|66217|5|Briefly described|p40.|||Rocks of this unit (Hickman 1983) were re-assigned to the Farrel Quartzite (Van Kranendonk et al. 2006a) in the Gorge Range area.||Unit in Gorge Creek Group.||||10-JUN-20
28476|Corboy Formation|66745|5|Briefly described|p53 Fig.3.|Mesoarchean|Mesoarchean|||Unit in Soanesville Group.||Overlies Cardinal Formation. Is overlain by Paddy Market Formation.|Coarse clastic rocks.|
28476|Corboy Formation|67197|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Soanesville Group.||||
28476|Corboy Formation|67201|4|Described|p7 Fig.4, p12 Tb.1|||In northern Pilbara Craton, East Pilbara Terrane, Soanesville Basin, rift-related successions.|c. 3190 Ma|Soanesville Group||||
28476|Corboy Formation|67269|5|Briefly described|p5|Paleoarchean|Paleoarchean|||Soanesville Group.|||Sandstone, shale and chert.|
28476|Corboy Formation|67668|6|Mentioned|Fig. 2; p. 154||Mesoarchean|East Pilbara Terrane, Pilbara Craton.||Soanesville Group||Underlies the Paddy Market Formation, overlies the Cardinal Formation|Clastic sediments.|
28476|Corboy Formation|68282|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton. The 5 facies are mapped separately.|c. 3190 Ma (Rasmussen et al. 2007).|Of the Soanesville Group|||Wacke and lithic arenite; quartz sandstone and quartzite; sandstone, siltstone and conglomerate; sandstone and minor interbedded conglomerate; all metamorphosed; intercalated psammopelitic schist and quartzite.|
28476|Corboy Formation|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Soanesville Basin. 8 facies are mapped separately.|c. 3190 Ma (Rasmussen et al., 2007)|Of the Soanesville Group.|||Includes schistose metasedimentary rock; psammitic and pelitic schist; pelite; pelitic schist containing andalusite; muscovite-bearing quartzite; pebble and cobble conglomerate; sandstone and minor interbedded conglomerate; wacke and lithic arenite.|30-APR-14
28476|Corboy Formation|69015|5|Briefly described|Map Legend|Mesoarchean|Paleoarchean|Pilbara Craton. Mapped as 8 unnamed sub-units. Age from a sandstone and minor interbedded conglomerate unit. See map legend for a detailed lithological description.|c.3190 Ma (Rasmussen et al. 2007).|Of the Soanesville Group.|||Intercalated psammite and mafic schist; pelite; quartzite; pebble and cobble conglomerate; sandstone and minor interbedded conglomerate; sandstone, siltstone, and local conglomerate; quartz sandstone and quartzite; wacke and lithic arenite.|02-MAY-14
28476|Corboy Formation|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|Age derived from sample of metamorphosed sandstone (142836.1.pdf) and constrains maximum age for deposition of sandstone protolith.|3426 Ma +/- 10 Ma (SHRIMP)|Soanesville Group|||Psammitic and pelitic schist, mica schist and quartzite. Intercalated psammopelitic schist and quartzite. Pelite, metasiltstone, mudstone and shale.  Pebble and cobble conglomerate, sandstone, siltstone, wacke and lithic arenite; all metamorphosed.|
28476|Corboy Formation|69301|5|Briefly described|p5 Fig.3, p9 Tb.1, p20 Tb.2|||Pilbara Craton. East Pilbara Terrane. Soanesville Basin. Rift-related successions.|3190 Ma|Soanesville Group||||
28476|Corboy Formation|69590|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Paleoarchean|Geological province: Pilbara Craton. Of Soanesville Basin. Events: Mosquito Creek Orogeny; North Pilbara Orogeny; Prinsep Orogeny; East Pilbara Terrane Rifting Event. Sample GSWA 142836 (metamorphosed sandstone) yielded an interpreted maximum depositional age of 3246+\-10 Ma (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|3228-3176 Ma (inferred)|Unit of Soanesville Group.|||Conglomerate and sandstone interlayered with ultramafic rock; pelite, pelitic and psammopelitic schist and quartzite,  sandstone and siltstone; metamorphosed.|
28476|Corboy Formation|69616|5|Briefly described|p161-164, p166, p180-181|Archean|Archean|Up to 200m thick at Kangaroo Caves. Characterised by abundant folds and bedding-parallel pinch and swell structures. Displacement up to tens of metres across both normal and reverse faults. Hydrothermal alteration discussed.||Unit in Soanesville Group.||Overlies Cardinal Formation and Sulphur Springs Group. Intrudes (neptunian sandstone dykes) into Marker Chert. Is overlain by Paddy Market Formation.|Coarse-grained turbiditic sandstones and minor interbedded turbiditic siltstones; local basal pebbly conglomerate.|12-OCT-15
28476|Corboy Formation|70022|6|Mentioned|p113, 115-116|||Soanesville Basin, East Pilbara Terrane.||Basal Soanesville Group.|||Feldspathic sandstone and metasandstone.|
28476|Corboy Formation|70775|5|Briefly described|p12|||East Pilbara.||Soanesville Group||Overlies the Cardinal Formation. Overlain by the Paddy Market Formation.||
28476|Corboy Formation|71041|5|Briefly described|p44, p45 fig 2|Mesoarchean|Mesoarchean|Basalts and BIFs have been reassigned to the Honeyeater Basalt. |3190 Ma|Soanesville Group||Intruded by the Dalton Suite.||
28476|Corboy Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Paleoarchean|Soanesville Basin.|max age ~3228 Ma, min age 3190+/-10 Ma.|Soanesville Group|||Siliciclastic sedimentary rocks; metamorphosed.|
28476|Corboy Formation|72251|5|Briefly described|p54|Mesoarchean|Mesoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Soanesville Group.||Overlain by Paddy Market Formation. Underlain by Budjan Creek Formation.||
28476|Corboy Formation|72668|5|Briefly described|p4-6|||East Pilbara Terrane.||Soanesville Group||Overlies the Pincunah Hill Formation. Overlain by the Paddy Market Formation.|Sandstone.|13-JAN-22
28476|Corboy Formation|73598|6|Mentioned|p1212|||East Pilbara Terrane.||Soanesville Group.||Overlies Budjan Creek Formation. Is overlain by Paddy Market Formation.||
30307|Corkwood Tonalite|22547|6|Mentioned|p13|||||||||
30307|Corkwood Tonalite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of Dougalls suite.  Age c. 1850 Ma||||||07-NOV-08
30307|Corkwood Tonalite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tickalara Metamorphics (Lamboo Complex).  Age: 1865-1850Ma.||||||07-NOV-08
30307|Corkwood Tonalite|43853|5|Briefly described|Map Legend||Proterozoic|||||||
30307|Corkwood Tonalite|43855|5|Briefly described|Map Legend||Proterozoic|||||||
30307|Corkwood Tonalite|44230|5|Briefly described|Map Legend||Proterozoic|||||||
30307|Corkwood Tonalite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
30307|Corkwood Tonalite|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Dougalls Suite.||||||07-NOV-08
30307|Corkwood Tonalite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Tickalara Metamorphics.|||Foliated and metamorphosed biotite (-hornblende) tonalite and granodiorite; locally garnet-bearing|
31892|Corrara Granite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs suite.||||||07-NOV-08
31892|Corrara Granite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs Supersuite. Age: 1825Ma. Geological province: Kimberley Province.||||||07-FEB-11
31892|Corrara Granite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  In the Bow River batholith.  Age: 1835-1805Ma.||||||07-NOV-08
31892|Corrara Granite|43854|5|Briefly described|Map Legend||Proterozoic|Of Sally Downs Supersuite.||||||14-OCT-08
31892|Corrara Granite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31892|Corrara Granite|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Syenite Camp Suite (Sally Downs Supersuite).||||||07-NOV-08
31892|Corrara Granite|66846|5|Briefly described|p558 Table 4|Orosirian|Orosirian|Age probably from U-Pb SHRIMP dating of zircon (see p547). |~1820 Ma|Of Syenite Camp suite.||||
31892|Corrara Granite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Syenite Camp Suite|||Medium-grained, equigranular biotite(-hornblende) tonalite.|30-JUL-15
31892|Corrara Granite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Syenite Camp Suite|||Medium grained, equigranular biotite-hornblende tonalite.|
31892|Corrara Granite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2.|1817-1817 Ma (Inferred)|Unit of Syenite Camp Suite.|||Medium-grained, equigranular biotite(-hornblende) tonalite|
31892|Corrara Granite|70154|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1817 Ma|Syenite Camp Suite|||Medium grained, equigranular biotite tonalite|
31892|Corrara Granite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1817 Ma (inferred)|Unit of Syenite Camp Suite.|||Medium-grained, equigranular biotite(-hornblende) tonalite|
31892|Corrara Granite|72437|6|Mentioned|p11, p100-p101|||||Syenite Camp Suite|Includes the Mabel Hill Tonalite''|||
80592|Corridor Gabbro|70731|5|Briefly described|p268,274,279|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. In contact with Paperbark Supersuite, characterised by back-veining and pillow-lava textures at contact zone, indicating mafic intrusion into still-cooling felsic rocks. Coeval with Springvale and Toby layered mafic intrusions within the Paperbark Supersuite and Marboo Formation during Hooper Orogeny.|c. 1855 Ma|||||
80592|Corridor Gabbro|70851|5|Briefly described|p3-p4, p16, 27|Paleoproterozoic|Paleoproterozoic|[Said to be of Blake et al. 2000a, BMR Bull 246, but they use Corridor gabbro p29 and in Ch5, p147]. Hooper Orogeny.|c. 1855 Ma|Paperbark Supersuite?||||10-AUG-18
31133|Corridor gabbro|23897|5|Briefly described|p377 Fig.1|||Informal name.||||||
31133|Corridor gabbro|43484|6|Mentioned|11|||||||||
31133|Corridor gabbro|60498|6|Mentioned|p1016 Fig.1.|Paleoproterozoic|Paleoproterozoic||||||Layered mafic-ultramafic intrusion:|
31133|Corridor gabbro|69585|5|Briefly described|p31|Orosirian|Orosirian|Central Lamboo Province. Geochemistry indicates mantle sources modified by subduction processes.|c.1830 Ma.||||Large layered mafic intrusion.|
31133|Corridor gabbro|70812|5|Briefly described|p6, p8, p20, p22, p43|Orosirian|Orosirian|Informal name. Western Zone of the Halls Creek Orogen, Lamboo Province.|c. 1850 Ma||||Mafic magmatics.|
83877|Cosmos Ultramafic sequence|69414|5|Briefly described|p85, 88-92, 100-103|Archean|Archean|Yilgarn Craton. Part of the succession at the Cosmos mine, but not part of the Agnew-Wiluna greenstone belt. Comprises two ultramafic packages. The lower is 2724 +/- 3 Ma to 2685 +/- 8 Ma, the upper is 2685 +/- 8 Ma to 2670 +/- 6 Ma; and they are separated by a 2685 +/- 8 Ma discontinuous felsic horizon. Hosts several massive and disseminated nickel sulfide deposits (detailed). 500m thinning to the N to <50m.|2724 +/- 3 Ma to 2670 +/- 6 Ma.||||Spinifex-textured komatiites, olivine-pyroxene cumulates, olivine orthocumulates, olivine mesocumulates and olivine adcumulates. Metamorphosed. Feldspar-phyric coherent dacites and andesite-dacite crystal tuffs.|
73854|Cossack Metabasite|24391|5|Briefly described|p8-5 Fig.2|Archean|Archean|Of Point Samson Group. Geological Province: Pilbara Block.||||||07-NOV-08
23512|Cossigny Member|13255|6|Mentioned|p369|Late Triassic|Middle Triassic|Roebuck Basin.||Unit in Keraudren Formation.||||
23512|Cossigny Member|13354|6|Mentioned|p377.|Early Triassic|Late Permian|Beagle Sub-basin.||17||||28-OCT-14
23512|Cossigny Member|41732|6|Mentioned|Fig.3|||||||||
23512|Cossigny Member|43173|6|Mentioned|54||Triassic|||||||
23512|Cossigny Member|44143|5|Briefly described|p448|Middle Triassic|Middle Triassic|Offshore Canning Basin. Dominantly limestone.||||||
23512|Cossigny Member|69297|6|Mentioned|p337, p339, p352|Norian|Carnian|Canning and Roebuck Basins. Potential hydrocarbon seal.||Keraudren Formation||Unconformably overlies the Grant Group.||
23512|Cossigny Member|70065|5|Briefly described|Rowley: Fig.2; p2. Regional: Fig.4; p3|Carnian|Ladinian|Roebuck Basin and offshore Canning Basin. Forms an intraformational seal. A high-amplitude seismic reflector.||Keraudren Formation.||Overlies Lower Keraudren Formation. Is overlain by Upper Keraudren Formation.|A widespread limestone unit.|
23512|Cossigny Member|70066|5|Briefly described|Dampier: Fig.2. Exmouth: Fig.2|Ladinian|Ladinian|See also Regional: Fig.6; p4. Northern Carnarvon Basin. A significant regional seismic marker, particularly in the Beagle Sub-basin.||Mungaroo Formation.|||Paralic and marine siltstone, claystone and limestone.|
72705|Cotton Well Granodiorite|64621|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite. Age: 3318-3312Ma. Muscovite granodiorite, fine- to medium-grained, weakly foliated; metamorphosed.||||||07-NOV-08
72705|Cotton Well Granodiorite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Emu Pool Supersuite. 3318-3312 Ma. Muscovite granodiorite; fine- to medium-grained; weakly foliated; metamorphosed.||||||
72705|Cotton Well Granodiorite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean||||||Muscovite granodiorite; fine- to medium-grained; weakly foliated; metamorphosed|
72705|Cotton Well Granodiorite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3318-3312 Ma (inferred)|Unit of Emu Pool Supersuite.|||Muscovite granodiorite; fine to medium grained; weakly foliated; metamorphosed|
72705|Cotton Well Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite|
72705|Cotton Well Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||Max age 3318+/-3 Ma, min 3309+/-4 Ma|Emu Pool Supersuite|||Muscovite granodiorite; fine to medium grained; weakly foliated; metamorphosed.|
32211|Coucal Formation|23416|5|Briefly described|Map Legend|Archean|Archean|Of Coonterunah Group, Pilbara Craton.||||||07-NOV-08
32211|Coucal Formation|23755|4|Described|p18|Archean|Archean|See also page 17 Table 1. Age: 3515+/-3 Ma. Of Coonterunah Group.||||||30-APR-13
32211|Coucal Formation|23783|5|Briefly described|p13 Fig. 7|||Of Coonterunah Group.||||||
32211|Coucal Formation|23813|5|Briefly described|p91 Tb. 1|Archean|Archean|Of the Coonterunah Group. Age: c.3.51 Ga (U-Pb SHRIMP). Geological Province: Pilbara Craton.||||||11-APR-13
32211|Coucal Formation|24025|4|Described|p9 Tb. 1|Archean|Archean|Of Coonterunah Group. Mafic and felsic volcanic rocks, chert, carbonate rocks, banded iron formation. Max. thickness: 1000 m. Geological Province: Pilbara Craton.||||||11-APR-13
32211|Coucal Formation|24166|4|Described|p9|Archean|Archean|Of the Coonterunah Group.||||||07-NOV-08
32211|Coucal Formation|24184|5|Briefly described|p699 Fig.3|Archean|Archean|Overlain by Double Bar Formation. Underlain by Table Top Formation. Geological Province: Pilbara Craton. Age: 3525 Ma (Buick et al 1995)||||||11-APR-13
32211|Coucal Formation|24327|5|Briefly described|Map Legend|Archean|Archean|Mafic schist and amphibolite. Of the Coonterunah Group. Age: 3515Ma. Geological Province: Pilbara Craton.||||||11-APR-13
32211|Coucal Formation|24349|5|Briefly described|Map legend|Archean|Archean|Of Coonterunah Group. Age: c.3515 Ma. Geological Province: Pilbara Craton||||||11-APR-13
32211|Coucal Formation|24531|5|Briefly described|p5|Archean|Archean|Of the Coonterunah Group (Pilbara Supergroup).  Age: c.3515 Ma (Buick et al, 1995).  Geological Province: Pilbara Craton.||||||11-APR-13
32211|Coucal Formation|24550|5|Briefly described|p31 Tb. 3.1|Archean|Archean|Of the Coonterunah Group. Mafic and felsic volcanics, chert, BIF. Age: 3515 Ma. Max. thickness: 6 km. Geological Province: Pilbara Craton.||||||11-APR-13
32211|Coucal Formation|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Of the Talga Talga Subgroup (Warrawoona Group). Mafic and felsic volcanic rocks, chert, carbonate, BIF.||||||07-FEB-11
32211|Coucal Formation|50379|5|Briefly described|Map Legend|Archean|Archean|Of Coonterunah Group (Pilbara Supergroup). Geological Province: Pilbara Craton. Age: c. 3515 Ma||||||07-NOV-08
32211|Coucal Formation|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Geological Province: eastern Pilbara Craton.||||||07-NOV-08
32211|Coucal Formation|61266|4|Described|p56-57 Fig.1, p58 Tb.1|Archean|Archean|Of the Coonterunah Group. Underlies Double Bar Formation. Overlies Table Top Formation. Thickness: ~100m. Consists of basalt, andesitic to felsic volcanic rocks, and interbedded black and white-layered cherty iron formations. Geol. Prov: Pilbara Craton.||||||11-APR-13
32211|Coucal Formation|61579|5|Briefly described|p58 Fig. 2|Archean|Archean|Of the Coonterunah Group. Age: 3515 Ma.||||||11-APR-13
32211|Coucal Formation|63420|5|Briefly described|Map legend|Archean|Archean|Of the Coonterunah Subgroup (Warrawoona Group, Pilbara Supergroup). Geological Province: Pilbara Craton. Amphibole; metamorphosed mafic volcanic and intrusive rocks, locally schistose.||||||11-APR-13
32211|Coucal Formation|63441|5|Briefly described|p4 Tb. 1, p19|Archean|Archean|Of Coonterunah Subgroup (Warrawoona Group, Pilbara Supergroup). Age: 3515+/-3Ma.||||||07-FEB-11
32211|Coucal Formation|63538|4|Described|p5, p8, p13, p18, p22, p6 Fig. 3|Archean|Archean|Of Coonterunah Subgroup. Underlain by Table Top Formation, overlain by Double Bar Formation. Geological Province: Pilbara Craton. Andesitic to dacitic volcanics and volcaniclastic units.||||||19-APR-13
32211|Coucal Formation|63649|5|Briefly described|p201 Fig. 2|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Age: 3.515Ga. Geological Province: Pilbara Craton.||||||07-FEB-11
32211|Coucal Formation|64328|5|Briefly described|p56 Tb. 1|||Of the Coonterunah Group. Felsic volcanic rocks, chert.||||||07-FEB-11
32211|Coucal Formation|64405|5|Briefly described|p4|Archean|Archean|Name inferred from Coucal only in Figure 3. Of the Warrawoona Group (De Grey Supergroup). Age: 3515 Ma. Felsic rocks.||||||11-APR-13
32211|Coucal Formation|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Coonterunah Subgroup. Age shown as 3515-3498 Ma. Felsic volcanic rocks; local felsic volcanic breccia; metamorphosed.||||||
32211|Coucal Formation|66217|5|Briefly described|p14. |||East Pilbara Terrane, Pilbara Craton. Not exposed on COONGAN map area.||Unit in Coonterunah Subgroup.||||
32211|Coucal Formation|66664|6|Mentioned|p7.||||||||Metafelsic volcanic rocks.|
32211|Coucal Formation|66745|5|Briefly described|pp53-54.|Paleoarchean|Paleoarchean||3515-3498 Ma.|Unit in Coonterunah Subgroup.||Overlies Table Top Formation. Is overlain by Double Bar Formation.|Felsic volcanic rocks.|
32211|Coucal Formation|67130|6|Mentioned|p13, p15 fig 10|Paleoarchean|Paleoarchean||3515 Ma|Warrawoona Group||Overlies Table Top Basalt, overlain by Double Bar Basalt|Dacite.|
32211|Coucal Formation|67197|5|Briefly described|p4-5, p8|Paleoarchean|Paleoarchean|East Pilbara Terrane.|c.3515 Ma.|Coonterunah Subgroup.|||Folded chert and volcanic rocks.|
32211|Coucal Formation|67201|4|Described|p7 Fig.4, p12 Tb.1|||In northern Pilbara Craton, East Pilbara Terrane.|c. 3515 Ma|Coonterunah Subgroup||||
32211|Coucal Formation|67269|5|Briefly described|p5-6|Paleoarchean|Paleoarchean||3515-3498 Ma.|Warrawoona Group.|||Felsic volcanic rocks and chert.|
32211|Coucal Formation|67270|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.|3515-3498 Ma.|Coonterunah Subgroup.||||
32211|Coucal Formation|67668|6|Mentioned|Fig. 2; p. 154||Paleoarchean|East Pilbara Terrane, Pilbara Craton.|3515 - 3500 Ma|Coonterunah Subgroup of the Warrawoona Group||Underlies the Double Bar Formation, overlies the Table Top Formation.||17-SEP-14
32211|Coucal Formation|68035|4|Described|p293|Paleoarchean|Paleoarchean|Pilbara Supergroup, East Pilbara Terrane. Includes the oldest known BIF in the Pilbara Craton.|3.515 - 3498 Ma|Of Coonterunah Subgroup||Overlies Table Top Formation, overlain by Double Bar Formation.|Basalt, felsic volcanic rocks, minor chert at base and top.|
32211|Coucal Formation|68280|5|Briefly described|p4||||3515-3498 Ma|Coonterunah Subgroup||Overlies Table Top Formation, overlain by Double Bar Formation|Felsic volcanic rocks, basalt and chert.|
32211|Coucal Formation|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|3515-3498 Ma (Buick et al. 1995).|Of the Coonterunah Subgroup.|||Rhyolite and rhyodacite; generally massive, quartz-feldspar porphyritic rock (metamorphosed); quartz-feldspar porphyritic rhyolite (metamorphosed).|
32211|Coucal Formation|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Age inferred from parent unit.||Of the Coonterunah Subgroup.|||Amphibolite, minor mafic schist (locally silicified); dominantly quartz- and feldspar-porphyritic rhyolite intrusive rock, subordinate felsic tuffaceous sandstone and quartz arenite; metamorphosed.|06-JAN-15
32211|Coucal Formation|68284|5|Briefly described|p7|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|3515-3498 Ma.|Coonterunah Subgroup.||Overlies Table Top Formation. Is overlain by Double Bar Formation.||
32211|Coucal Formation|69013|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane. 3 facies are mapped separately.|3515-3498 Ma (Buick et al., 1995)|Of the Coonterunah Subgroup.|||Amphibolite and mafic schist (locally silicified); ferruginous chert (includes cherty banded iron-formation and layered chert; metamorphosed); basalt and andesite (locally schistose; metamorphosed).|30-APR-14
32211|Coucal Formation|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.  Includes 2 unnamed sub-units.|c.3515 (Buick et al. 1995)|Of the Coonterunah Subgroup.|||Felsic volcanic rocks; local felsic volcanic breccia; ferruginous chert, including cherty banded iron-formation and layered chert; basalt and andesite, locally schistose; all metamorphosed.|02-MAY-14
32211|Coucal Formation|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Rhyolite and rhyodacite, quartz-feldspar porphyritic rhyolite, basalt and andesite; metamorphosed.||Coonterunah Subgroup|||Felsic volcanic rocks; local felsic volcanic breccia; metamorphosed. Amphibolite and mafic schist; locally silicified. Ferruginous chert, includes cherty banded iron formation and layered chert.|
32211|Coucal Formation|69301|4|Described|p5 Fig.3, p9 Tb.1, p19, p20 Tb.2|||Pilbara Craton. East Pilbara Terrane. The oldest known BIF in Pilbara Craton occurs in Coucal Formation (ca 3.52 Ga) of lower Warrawoona Group. Every BIF unit potentially testifies to bacteria in the depositional environment.|3515-3498 Ma|Coonterunah Subgroup|||Basalt and felsic volcanic rocks.|
32211|Coucal Formation|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.|3515-3490 Ma (inferred)|Unit of Coonterunah Subgroup.|||Amphibolite and mafic schist; locally silicified, Basalt and andesite; locally schistose; metamorphosed, ferruginous chert and cherty BIF, layered chert, qtz-feldspar porphyritic rhyolite, dacite.|
32211|Coucal Formation|70022|6|Mentioned|p115|||East Pilbara Terrane.||Coonterunah Subgroup.||||
32211|Coucal Formation|70775|5|Briefly described|p12|Paleoarchean|Paleoarchean|East Pilbara.|c. 3515 Ma|Warrawoona Group||Overlies the Table Top Formation. Overlain by the Double Bar Formation.||
32211|Coucal Formation|70884|5|Briefly described|p123|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|3.52-3.50 Ga|Unit of Coonterunah Subgroup.||Overlain by Double Bar Formation. Underlain by Table Top Formation.||
32211|Coucal Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Warrawoona  Large Igneous Province.|Max age 3515+/-3 Ma, min 3498+/-2 Ma.|Coonterunah Subgroup|||Felsic volcanic rocks; local felsic volcanic breccia; metamorphosed.|
32211|Coucal Formation|72064|5|Briefly described|p66|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawoona Group.||Overlain by Double Bar Formation. Underlain by Table Top Formation.||
32211|Coucal Formation|72251|5|Briefly described|p54|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unt of Coonterunah Subgroup.||Overlain by Double Bar Formation. Underlain by Table Top Formation.||
32211|Coucal Formation|72668|5|Briefly described|p3-8|||East Pilbara Terrane.||Coonterunah Subgroup||Overlies the Table Top Formation. Overlain by the Double Bar Formation.|Dacite dominated deposits.|
32211|Coucal Formation|73598|6|Mentioned|p1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Coonterunah Subgroup.||Overlies Table Top Formation. Is overlain by Double Bar Formation.||
79004|Courin Granodiorite|70226|5|Briefly described|Map legend.|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Carton.|c. 2742 Ma (Fletcher and McNaughton, 2002).|Rothsay Suite|||Migmatitic metatonalite with stromatic mesosomes of metatonalite and leucosomes of metamonzogranite; rare melanosomes of biotite metadiorite. Interlayered monzogranitic augen gneiss and granodiorite schist on a metre-scale; locally lineated.|16-DEC-15
79004|Courin Granodiorite|70796|5|Briefly described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. See also 100K_interpgeop_lut.csv, 500k_interpgeop_lut.csv, Yalgoo100_2241_stratig.pdf. Numerous additional lithologies are discussed.|ca 2742 Ma (inferred)|Rothsay Suite|||Migmatitic metatonalite with stromatic mesosomes of metatonalite and leucosomes of metamonzogranite; rare melanosomes of biotite metadiorite. Interlayered monzogranitic augen gneiss and granodiorite schist on a metrescale; locally lineated.|
79004|Courin Granodiorite|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.|2742 Ma (inferred)|Unit of Rothsay Suite.|||Migmatitic metatonalite with stromatic mesosomes of metatonalite and leucosomes of metamonzogranite; rare melanosomes of biotite metadiorite; Interlayered monzogranitic augen gneiss and granodiorite schist on a metre-scale; locally lineated.|
78360|Courlbarloo Tonalite|69584|6|Mentioned|p2, p60, Plate 1|Mesoarchean|Mesoarchean|Intrudes unnamed basaltic and andesitic rocks which host the deposits of the Just Desserts-Trajan area and C Zone. These unnamed rocks may be equivalent to the Norie Group.|2813 +/- 5 Ma (Cassidy et al, 2002)|Mount Kenneth Suite||||
78360|Courlbarloo Tonalite|70140|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c.2813 Ma (Cassidy et al., 2002).|Mount Kenneth Suite.|||Hornblende tonalite with 3-8mm hornblende phenocrysts; locally weakly deformed; metamorphosed.|
78360|Courlbarloo Tonalite|70796|5|Briefly described|100k_geologyp_lut.csv|Mesoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_interpgeop_lut.csv,  500k_interpgeop_lut.csv, Youanmi100_2640_stratig.pdf.|2813 +/ 5 Ma (inferred)|Mount Kenneth Suite|||Hornblende tonalite with 38 mm hornblende phenocrysts; locally weakly deformed; metamorphosed.|
78360|Courlbarloo Tonalite|71168|5|Briefly described|p7, p59|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Age provided is a SHRIMP U-Pb zircon date and constrains the age of the Parent Mount Kenneth Suite.|2813 +/- 3 Ma (Fletcher and McNaughton, 2002)|Mount Kenneth Suite||||
78360|Courlbarloo Tonalite|71269|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.|2813+\-5 Ma (isotopic)|Unit of Mount Kenneth Suite.|||Hornblende tonalite with 3-8 mm hornblende phenocrysts; locally weakly deformed; metamorphosed|
26500|Cowan Dolomite|14227|5|Briefly described|Enclos. 2|Late Oligocene|Late Oligocene|Presented as Revenge FM + Cowan Dolomite.||||||07-FEB-11
26500|Cowan Dolomite|22769|5|Briefly described|Table1p759||Oligocene|||||||
26500|Cowan Dolomite|23797|5|Briefly described|p3|Tertiary|Tertiary|Of the Redmine Group. Max age: Late Tertiary. Min age: Late Tertiary. Geological Province: Yilgarn Craton.||||||17-FEB-05
26500|Cowan Dolomite|23817|5|Briefly described|p430, 431|Late Eocene|Late Eocene|Geological Province: Bremer Basin.  Of the Eundynie Group.  Max. Thickness: 12m.||||||
26500|Cowan Dolomite|23989|5|Briefly described|p54 Fig. 46|Cenozoic|Cenozoic|||||||21-APR-09
26500|Cowan Dolomite|30144|6|Mentioned|p84|||Depositional history||||||
26500|Cowan Dolomite|30268|6|Mentioned|p44|||||||||
26500|Cowan Dolomite|30562|4|Described|p6|||Tertiary age. See also p19.||||||15-AUG-06
26500|Cowan Dolomite|30959|6|Mentioned|Map legend|Eocene|Eocene|||||||
26500|Cowan Dolomite|32648|6|Mentioned|p32|||U. Eocene||||||
26500|Cowan Dolomite|34999|6|Mentioned|Table 17|||||||||
26500|Cowan Dolomite|36890|3|Fully described|p431|||||||||
26500|Cowan Dolomite|40877|5|Briefly described|p55|||||||||
26500|Cowan Dolomite|41771|6|Mentioned|p49|||See also Fig.6||||||
26500|Cowan Dolomite|42108|5|Briefly described|p122|||See also Fig.6||||||
26500|Cowan Dolomite|42817|5|Briefly described|p29|||Of Eundynie Group.||||||15-AUG-06
26500|Cowan Dolomite|42959|4|Described|p63|||See also p58 Fig 3.||||||15-AUG-06
26500|Cowan Dolomite|43065|5|Briefly described|Fig.5,p92|Late Eocene|Middle Eocene|||||||
26500|Cowan Dolomite|43838|5|Briefly described|p4||Tertiary|Lacustrine. Within Redmine Group.||||||12-JUL-16
26500|Cowan Dolomite|64646|6|Mentioned|p23 Fig. 3|Miocene|Miocene|||||||08-FEB-10
26500|Cowan Dolomite|65194|5|Briefly described|p135, p136 Fig.4.37|||Post-Eocene sediments in Cowan Palaeovalley. Includes white to buff-coloured dolomite and dolomitic carbonate mudstone.||||||
26500|Cowan Dolomite|69152|4|Described|1m_geologyp08_lut.csv|Late Eocene|Late Eocene|||Redmine Group|||Massive, cryptocrystalline white or grey dolomite.|05-AUG-15
26500|Cowan Dolomite|69598|6|Mentioned|p9, p10|Middle Miocene|Early Miocene|||Redmine Group|||Interbedded lacustrine carbonates.|
26500|Cowan Dolomite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolostone|
26500|Cowan Dolomite|71270|5|Briefly described|1m_geologyp12_lut.csv|||Geological province: Yilgarn Craton, West Australian Craton. ||Unit of Redmine Group.|||Massive, cryptocrystalline white or grey dolomite|
26500|Cowan Dolomite|71788|14|Not recorded|p97-98, Plate 41 ||Eocene|||||||
40167|Cowaramup Gneiss|24542|5|Briefly described|p7|Neoproterozoic|Mesoproterozoic|Strongly deformed and metamorphosed composite of interleaved anorthosite, leucogabbro, gabbro, sheets of granite and pagmatite veins. Of Leeuwin Complex.||||||
40167|Cowaramup Gneiss|24595|5|Briefly described|p588|||Banded gneiss of Myers (1994).  Part of the Leeuwin Complex.  Previously referred to as the Bunker Bay Suite (Kay, 1958).  Forms the core within the Hamelin Granite.  Geological Province: Leeuwin Block.||||||
26501|Coyrie Formation|12733|6|Mentioned|p562.|||Contains potential hydrocarbon sealing units.||||||
26501|Coyrie Formation|14228|6|Mentioned|p8, p18|Kungurian|Kungurian|||Byro Group||||
26501|Coyrie Formation|23174|5|Briefly described|Fig5p8|Permian|Permian|||||||
26501|Coyrie Formation|23279|6|Mentioned|p16|||||||||
26501|Coyrie Formation|23311|5|Briefly described|map legend|Artinskian|Artinskian|Of Byro Group.||||||
26501|Coyrie Formation|23312|5|Briefly described|map legend|Artinskian|Artinskian|Of Byro Group.||||||
26501|Coyrie Formation|23403|4|Described|p8|Early Permian|Early Permian|Of Byro Group.||||||
26501|Coyrie Formation|23569|4|Described|p4 Tb. 1|Early Permian|Early Permian|Parent: Byro Group.   Bioturbated siltstone and fine-grained sandstone.||||||
26501|Coyrie Formation|23726|5|Briefly described|p47|Early Permian|Early Permian|Overlying unit Mallens Sandstone. Underlying unit Billidee Formation. Geological Province: Carnarvon Basin.||||||
26501|Coyrie Formation|23815|4|Described|p284|Artinskian|Artinskian|Geological Province: Merlinleigh Sub-basin. Of the Newman Subgroup. Overlying unit: Mallens Greywacke (conformable). Underlying unit: Billidee Formation (conformable). Max. thickness: 400 m. Extremely fossiliferous.||||||
26501|Coyrie Formation|24044|5|Briefly described|p541 Fig.2|Early Permian|Early Permian|Of Byro Group.||||||
26501|Coyrie Formation|24114|5|Briefly described|p8|||Of Byro Group.||||||
26501|Coyrie Formation|30545|6|Mentioned|Fig.2|||Artinskian||||||
26501|Coyrie Formation|32113|6|Mentioned|p47|||||||||
26501|Coyrie Formation|32648|6|Mentioned|p32|||Byro Gp.||||||
26501|Coyrie Formation|32945|6|Mentioned|p90|||Permian||||||
26501|Coyrie Formation|33594|6|Mentioned|p37|||||||||
26501|Coyrie Formation|33701|6|Mentioned|Fig.1|||Artinskian.||||||
26501|Coyrie Formation|33710|6|Mentioned|Fig.1|||||||||
26501|Coyrie Formation|34532|6|Mentioned|p225|||Byro Group||||||
26501|Coyrie Formation|35105|6|Mentioned|Fig.66|||||||||
26501|Coyrie Formation|36020|6|Mentioned|p392|||||||||
26501|Coyrie Formation|36257|6|Mentioned|Table 2.1|||||||||
26501|Coyrie Formation|36890|3|Fully described|p284|||||||||
26501|Coyrie Formation|37000|6|Mentioned|p23|||||||||
26501|Coyrie Formation|37294|6|Mentioned|p100|||||||||
26501|Coyrie Formation|37295|6|Mentioned|p54|||||||||
26501|Coyrie Formation|37304|6|Mentioned|p55|||||||||
26501|Coyrie Formation|38493|3|Fully described|p36|||||||||
26501|Coyrie Formation|38494|4|Described|p29|||||||||
26501|Coyrie Formation|38917|6|Mentioned|p171|||||||||
26501|Coyrie Formation|39223|6|Mentioned|p242|||||||||
26501|Coyrie Formation|39316|6|Mentioned|Fig.2|||||||||
26501|Coyrie Formation|39370|6|Mentioned|Table 2|||||||||
26501|Coyrie Formation|39427|6|Mentioned|Table 1|||||||||
26501|Coyrie Formation|40336|6|Mentioned|p18|||||||||
26501|Coyrie Formation|40339|6|Mentioned|Map legend|Artinskian|Artinskian|||||||
26501|Coyrie Formation|40617|6|Mentioned|Fig.1|||||||||
26501|Coyrie Formation|41044|6|Mentioned|p134|||||||||
26501|Coyrie Formation|41271|3|Fully described|p94|||||||||
26501|Coyrie Formation|41438|6|Mentioned|Fig.11|||||||||
26501|Coyrie Formation|42116|5|Briefly described|p35|||See also Fig.14||||||
26501|Coyrie Formation|42392|6|Mentioned|p117|||Byro Group||||||
26501|Coyrie Formation|42462|6|Mentioned|p56|||||||||
26501|Coyrie Formation|42540|6|Mentioned|Table 2 P314|||||||||
26501|Coyrie Formation|42994|6|Mentioned|p37|||Also p53.||||||
26501|Coyrie Formation|43015|5|Briefly described|Table 1,p319|||||||||
26501|Coyrie Formation|43050|5|Briefly described|p26|||||||||
26501|Coyrie Formation|43255|5|Briefly described|map legend||Artinskian|Of Byro Group.||||||15-DEC-08
26501|Coyrie Formation|43256|5|Briefly described|5-22||Permian|||||||
26501|Coyrie Formation|43471|14|Not recorded|p239|||Megadesmus, Astartila||||||
26501|Coyrie Formation|43495|6|Mentioned|13|||||||||
26501|Coyrie Formation|43835|5|Briefly described|Map Legend||Artinskian|||||||
26501|Coyrie Formation|43882|14|Not recorded|p95|||Ammonoid.||||||
26501|Coyrie Formation|44219|14|Not recorded|p31||Artinskian|||||||
26501|Coyrie Formation|44344|14|Not recorded|p.10-12,24,opp.4,map||Artinskian|Artinskian; basal fm of Newman Subgroup (Byro Group). (G50-1).||||||
26501|Coyrie Formation|44345|14|Not recorded|map legend||Artinskian|||||||
26501|Coyrie Formation|44532|4|Described|p.7,8, map|||(G50-5).||||||
26501|Coyrie Formation|44533|5|Briefly described|map legend||Artinskian|Artinskian.||||||
26501|Coyrie Formation|44537|14|Not recorded|map legend||Artinskian|||||||
26501|Coyrie Formation|44657|14|Not recorded|p.5,6,9|||||||||
26501|Coyrie Formation|44994|6|Mentioned|Fig.7|||Correlation Perm.||||||
26501|Coyrie Formation|45015|5|Briefly described|map legend|Artinskian|Artinskian|Of the Newman Sub-Group (Byro Group). Geological Province: Carnarvon Basin.||||||31-MAY-06
26501|Coyrie Formation|45016|2|Defined|p.126-131||Artinskian|Tb, p.77,81,85,89,92-94,96,124,125,135-137,143,144,152,154. (F50-9,13,F49-16,G50-1,5,G49-4).||||||
26501|Coyrie Formation|48831|14|Not recorded|p.63|||On many pages. p.23,24,36,38,41,63,71,75||||||
26501|Coyrie Formation|48848|14|Not recorded|p.61,75|||||||||
26501|Coyrie Formation|49644|5|Briefly described|Table|||||||||
26501|Coyrie Formation|60331|5|Briefly described|p33 Fig.2|Artinskian|Artinskian|Of the Byro Group. Overlies Wooramel Group. Overlain by Mallens Sandstone. Geological Province: Southern Carnarvon Basin.||||||
26501|Coyrie Formation|61958|5|Briefly described|Map sheet 1|Artinskian|Artinskian|Of the Newman Sub-Group (Byro Group).||||||21-MAR-06
26501|Coyrie Formation|64580|5|Briefly described|map legend|||Of Lower Byro Group. Fine-grained biturbated sandstone overlying interbedded sandstone, siltstone and mudstone.||||||15-DEC-08
26501|Coyrie Formation|64630|6|Mentioned|p35 |||N.B. Lowermost Byro Group.||||||
26501|Coyrie Formation|64974|6|Mentioned|p147 Fig. 5|Artinskian|Artinskian|Geological Province: Carnarvon Basin.||||||24-JUN-09
26501|Coyrie Formation|66579|5|Briefly described|Map legend|Permian|Permian|Southern Carnarvon Basin.||Unit in Byro Group.||Is overlain by Mallens Sandstone.|Black shale, siltstone, and sandstone in coarsening-upward succession.|
26501|Coyrie Formation|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes brown sandstone, minor bioturbation; pale pink/tan sandstone, no bioturbation.|22-DEC-22
26501|Coyrie Formation|67200|5|Briefly described|p7 fig 5, p18 table 1|Kungurian|Artinskian|Thermal conductivity of 2.62 W/mK. See also p47, p54, app 2 p6. ||Byro Group||Overlies Billidee Formation, overlain by Mallens Sandstone|Interbedded sandstone and siltstone; trough cross beds, hummocky stratification and crude bedding.|
26501|Coyrie Formation|69011|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin.||Of the Byro Group.||Overlain by the Mallens Sandstone. Underlain by the Billidee Formation.|Comprises black shale, siltstone, and sandstone in coarsening-upward succession.|
26501|Coyrie Formation|69028|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin. Mapped with Mallens Sandstone as one unit.||Of the Byro Group.|||Fine-grained bioturbated sandstone overlying interbedded sandstone, siltstone and mudstone.|15-AUG-18
26501|Coyrie Formation|69166|4|Described|geologyp_lut.csv|Kungurian|Artinskian|||Byro Group|||Black shale, siltstone, and sandstone in coarsening-upward succession|
26501|Coyrie Formation|69182|6|Mentioned|Ch3 p55|||||||Overlies the Billidee Formation.||
26501|Coyrie Formation|69583|5|Briefly described|p130, p134 Fig.3, p135, Plates 3, 4|Permian|Permian|Southern Carnarvon Basin. Mapped as one unit with Mallens Sandstone. Seismic interpretation.||Byro Group.|||Fine-grained bioturbated sandstone overlain by interbedded sandstone, siltstone and mudstone.|
26501|Coyrie Formation|70795|4|Described|100k_geologyp_lut.csv|Kungurian|Artinskian|Also 100k_interpgeop_lut.csv|290-283 Ma|Byro Group|||Black shale, siltstone, and sandstone in coarsening-upward succession.|
26501|Coyrie Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, claystone, greywacke|
26501|Coyrie Formation|72910|4|Described|p6-9, p14, p16, p18, p23, p30, p39.|Kungurian|Artinskian|Thickness 85-200m. Type section is located in Northern Kennedy Range, 24d06m00sS; 115d08m30sE. See also p32-33, p41-42. Said to be Artinskian age p39.||Byro Group.||Conformably overlies Billidee, Keogh Formations.|Interbedded grey-black siltstone and fine sandstone, minor black shale.|
74633|Crab Creek Calcilutite Member|64449|2|Defined|p75, p79 Tb. 5|Holocene|Holocene|Of Sandfire Calcilutite. Consists of white/cream shelly, laminated to burrow-structured calcilutite; underlies mid-low tidal flats.||||||07-FEB-11
74633|Crab Creek Calcilutite Member|73213|5|Briefly described|958 Fig.3(a)|||||Sandfire Calcilutite.||Overlies Djugun Member. Is overlain by Lagrange Calcilutite Member.||
77465|Crane Formation|67370|6|Mentioned|p313 Fig.2. |Triassic|Triassic|||||Overlies Osprey Formation.||
77106|Crispin Mylonite|65419|5|Briefly described|pp5-6.|Paleoproterozoic|Paleoproterozoic|Of Pirajno and Occhipinti (in prep.). Their preferred term for a mylonitic unit named by Gee (1987) as Crispin Conglomerate.||Unit in Peak Hill Schist.|||Quartzite clasts in a matrix of quartz-sericite schist; both mylonitized.|
77106|Crispin Mylonite|70804|5|Briefly described|p5, p23|||Previously the Crispin Conglomerate of Gee (1987).|||||Mylonite with square to rounded quartz arenite clasts in a sericite-rich matrix.|
25865|Cronin Sandstone|7433|4|Described|p25 Fig.2, p42, p45. |Cretaceous|Jurassic|Officer Basin, southwest Canning Basin. Fluvial clastics. Contains plant fossils. Possible equivalent to Callawa Formation. Possibly diachronous, as part of it resembles Anketell Sandstone.||||Overlies Permian rocks in Canning Basin. Is overlain disconformably by Anketell Sandstone.|Bioturbated and cross-bedded sandstone; minor mudstone and conglomerate.|
25865|Cronin Sandstone|35387|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
25865|Cronin Sandstone|35902|4|Described|Table 1|||||||||
25865|Cronin Sandstone|35903|6|Mentioned|p7|||||||||
25865|Cronin Sandstone|36890|6|Mentioned|p350|||||||||
25865|Cronin Sandstone|38878|6|Mentioned|Map legend|Neocomian|Tithonian|Tithonian - Neocomian||||||
25865|Cronin Sandstone|44866|5|Briefly described|Map Legend||Cretaceous|||||||
25865|Cronin Sandstone|44998|2|Defined|p.128-130||Jurassic|(new name). Overlies Paterson Formation & Pc. On many pages. p.77,185, map, App.1 p257,261,App.6 p296.||||||
25865|Cronin Sandstone|45153|2|Defined|App.6-114|Late Jurassic|Middle Jurassic|Middle to Late Jurassic.||||||
25865|Cronin Sandstone|45158|3|Fully described|p14|||See also P13||||||
25865|Cronin Sandstone|49895|4|Described|p10|Jurassic|Late Triassic|Geological Province: Canning and Gunbarrel Basins, and Paterson Orogen. Overlies the Paterson Formation. Late Triassic or Jurassic in age. See also p6 Fig.3.||||||23-JAN-07
25865|Cronin Sandstone|49911|5|Briefly described|Map legend|Cretaceous|Cretaceous|Sandstone, fine- to coarse-grained, bioturbated, and cross-bedded; minor pebble conglomerate, plant fossils.  Geological Province: Canning Basin||||||
25865|Cronin Sandstone|67202|5|Briefly described|p69-71|Early Cretaceous|Late Jurassic|Fluvial deposits.||||Correlative of Callawa Formation.|Fine- to coarse-grained, bioturbated sandstone, minor conglomerate, mudstone.|
25865|Cronin Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone|
31789|Crooked Creek Granite|22547|4|Described|p11||Orosirian|Of Paperbark supersuite.||||||08-AUG-06
31789|Crooked Creek Granite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.||||||07-NOV-08
31789|Crooked Creek Granite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1850Ma. Geological province: Kimberley Province (East).||||||07-FEB-11
31789|Crooked Creek Granite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
31789|Crooked Creek Granite|43853|5|Briefly described|Map Legend||Proterozoic|||||||
31789|Crooked Creek Granite|44230|5|Briefly described|Map Legend||Proterozoic|||||||
31789|Crooked Creek Granite|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Paperbark Supersuite.||||||07-NOV-08
31789|Crooked Creek Granite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Paperbark Supersuite|||Medium-grained, porphyritic, biotite granodiorite and monzogranite.|30-JUL-15
31789|Crooked Creek Granite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 100k_xsecgeop_lut.csv||Paperbark Supersuite|||Medium grained, porphyritic, biotite granodiorite and monzogranite|22-SEP-17
31789|Crooked Creek Granite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone.|1864-1854 Ma (Inferred)|Unit of Paperbark Supersuite.|||Medium-grained, porphyritic, biotite granodiorite and monzogranite|
31789|Crooked Creek Granite|69925|6|Mentioned|p21|||||||Correlated with Dneiper Granite.||
31789|Crooked Creek Granite|70154|6|Mentioned|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1854-1864 Ma|Paperbark Supersuite||||
31789|Crooked Creek Granite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1864-1854 Ma (inferred)|Unit of Paperbark Supersuite.|||Medium-grained, plagioclase-phyric, biotite granodiorite and monzogranite|
31789|Crooked Creek Granite|72437|5|Briefly described|p88-89|||Lamboo Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Biotite monzogranite.|
74828|Crossroads Granodiorite|64891|5|Briefly described|p37 Fig. 2, p42, p50-51 Tb. 1|Archean|Archean|Of Big Bell Suite (Austin Downs Supersuite). Age: 2702+/-6Ma. Geological province: Murchison Domain. Monzogranite, commonly foliated; metamorphosed.||||||07-FEB-11
74828|Crossroads Granodiorite|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c.2702 Ma.|Unit in Big Bell Suite.|||Metagranodiorite, commonly foliated.|
74828|Crossroads Granodiorite|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. Mafic tonalite gneiss dated. U-Pb zircon age of 2724 +/- 2 Ma interpreted as the magmatic crystallization age of the tonalite. See geochron file 185923.1.pdf||Big Bell Suite|Includes 2 unnamed subunits.||Metagranodiorite to metamonzogranite; commonly foliated|
74828|Crossroads Granodiorite|69583|5|Briefly described|p49, p52; Plate 2|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Big Bell Suite.|||Metagranodiorite.|
74828|Crossroads Granodiorite|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean|||Big Bell Suite|||Granodiorite.|
74828|Crossroads Granodiorite|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Big Bell Suite.||||
74828|Crossroads Granodiorite|69627|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton||Big Bell Suite|||Biotite metagranodiorite; strongly foliated; commonly with pegmatite veins and other intrusive granitic phases.|
74828|Crossroads Granodiorite|70796|5|Briefly described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_interpgeop_lut.csv., 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 185923.1.pdf.|ca 2735 to 2711 Ma (inferred)|Big Bell Suite|||Metagranodiorite to metamonzogranite; commonly foliated. Pegmatitelayered metamonzogranite gneiss. Biotite metagranodiorite.|
74828|Crossroads Granodiorite|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). Wingate et al., 2011 provided a U-Pb SHIRMP crystallisation age of 2724+\-2 Ma for a sample from a tonalitic dyke. Sample GSWA 185923 (bt-hbl tonaltie gneiss) yielded a weighted mean 207Pb/206Pb date of 2724+\-2 Ma, interpreted to be magmatic crystallisation age. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv.|2735-2690 Ma (inferred)|Unit of Big Bell Suite.||Intruded by monzogranitic dykes of the Tuckanarra Suite.|Metagranodiorite to metamonzogranite; commonly foliated, pegmatite-layered.|
74828|Crossroads Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Youanmi Terrane.||Big Bell Suite|||Metagranodiorite to metamonzogranite; commonly foliated.|
23522|Crowbar Granodiorite|22534|4|Described|p11|||||||||
23522|Crowbar Granodiorite|22539|5|Briefly described|Map legend|Archean|Archean|||||||07-NOV-08
23522|Crowbar Granodiorite|41786|6|Mentioned|Table 2|||||||||
23522|Crowbar Granodiorite|43214|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
23522|Crowbar Granodiorite|43232|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
23522|Crowbar Granodiorite|43496|6|Mentioned|13|||||||||
23522|Crowbar Granodiorite|60076|5|Briefly described|p45 App. 1|||[Aggcb]   Medium- to coarse-grained, equigranular granodiorite.||||||13-APR-05
23522|Crowbar Granodiorite|65204|6|Mentioned|p17 Tbl.2, p18|Neoarchean||1-7mm grains; equigranular; U-Pb zircon age 2657+/-5 Ma.||||||
23522|Crowbar Granodiorite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Medium- to coarse-grained, equigranular granodiorite.||||||07-FEB-11
23522|Crowbar Granodiorite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Medium- to coarse-grained, equigranular granodiorite; domal within regional anticline; pervasive foliation.|05-AUG-15
23522|Crowbar Granodiorite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Medium- to coarse-grained, equigranular granodiorite; domal within regional anticline; pervasive foliation.|
23522|Crowbar Granodiorite|71270|4|Described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton.|||||Medium- to coarse-grained, equigranular granodiorite; domal within regional anticline; pervasive foliation|
39658|Cudalgarra Member|24449|2|Defined|p751 App. 1|Llanvirnian|Llanvirnian|Limestones, dolostones and evaporitic mudstones. Of the Nita Formation. Overlain by Bongabinni Formation; overlies the Leo Member conformably.  Max. thickness: 21m.  Geological Province: Canning Basin.  See also p745 and p743 Fig. 5. Type seciton  in CRA Exploration P/L mineral exploration hole DD87SS7 from 1463.6 to 1482.9 m. Boundaries probably diachronus.||||||02-MAR-20
39658|Cudalgarra Member|64643|5|Briefly described|p3 Fig. 2|Darriwilian|Darriwilian|Of Nita Formation?||||||
39658|Cudalgarra Member|65449|3|Fully described|p5-6, p8, p17, p49-50; Plates 1-11|Darriwilian|Darriwilian|Of McCracken (1994). From a sequence stratigraphy perspective, this unit belongs genetically with the Carribuddy Group.||Of Nita Formation.||Overlies Leo Member. Is overlain by Bongabinni Formation.|Shaling-upward trend.|09-APR-20
39658|Cudalgarra Member|69883|4|Described|p5, p10, p12, p14, p27, |||Western Canning basin. The stratotype for this member is within DD87SS7. 12-21m thick.  A reference section is interpreted in Great Sandy 1 (1447-1467m). See also plate 1-3.||Nita Formation||||02-MAR-20
27756|Cuddingwarra Formation|30491|5|Briefly described|p8|||Archaean age||||||
27756|Cuddingwarra Formation|30882|4|Described|p47|||Stratigraphy||||||
27756|Cuddingwarra Formation|30960|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
27756|Cuddingwarra Formation|31222|6|Mentioned|p13|||||||||
27756|Cuddingwarra Formation|31223|6|Mentioned|p580|||||||||
27756|Cuddingwarra Formation|35269|6|Mentioned|p298|||||||||
27756|Cuddingwarra Formation|36870|3|Fully described|p56|||||||||
27756|Cuddingwarra Formation|38492|5|Briefly described|Table 2|||||||||
27756|Cuddingwarra Formation|41066|6|Mentioned|1 of 2 N03|||||||||
27756|Cuddingwarra Formation|41841|5|Briefly described|Table 1|||Article recommends adandoning this name use. See p55||||||
74821|Cue Tonalite|64891|5|Briefly described|p37 Fig. 2, p41, p50-51 Tb. 1|Archean|Archean|Of Cullculli Suite (Annean Supersuite). Age: 2759+/-4Ma. Geological province: Murchison Domain. Tonalite; metamorphosed.||||||07-FEB-11
74821|Cue Tonalite|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c.2759 Ma (Wang 1998 PhD thesis unpub.).|Unit in Cullculli Suite.|||Medium- to coarse-grained, metamorphosed leucocratic tonalite.|
74821|Cue Tonalite|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane||Cullculli Suite|||Leucocratic tonalite; medium to coarse-grained; metamorphosed|
74821|Cue Tonalite|69583|5|Briefly described|p49; Plate 2|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Cullculli Suite.|||Leucocratic tonalite, metamorphosed.|
74821|Cue Tonalite|69584|5|Briefly described|p5 Fig.2|Neoarchean|Neoarchean|||CullCulli Suite|||Tonalite.|
74821|Cue Tonalite|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Cullculli Suite.||||
74821|Cue Tonalite|70796|5|Briefly described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. See also 100K_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv. Numerous additional lithologies are discussed.|ca 2787 to 2735 Ma (inferred)|Cullculli Suite|||Leucocratic tonalite; medium to coarse grained; metamorphosed|
74821|Cue Tonalite|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv.|2787-2735 Ma|Unit of Cullculli Suite.|||Leucocratic tonalite; medium to coarse grained; metamorphosed|
74821|Cue Tonalite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Youanmi Terrane.||Cullculli Suite|||Leucocratic tonalite; medium to coarse grained; metamorphosed.|
74815|Cullculli Suite|64891|4|Described|p37 Fig. 2, p41, p48-9 Tb. 1|Archean|Archean|Of Annean Supersuite. Includes Mindoola, Burnakura + Cue Tonalites, Reedys Trondhjemite, Snake Gully, Racecourse, Nannine + Triton Tonalites. Age: 2785-2744Ma. In Murchis.Dom. Hornblende (-biotite) tonalite-trondhjemite-granodiorite + qtz-diorite rocks||||||07-FEB-11
74815|Cullculli Suite|65548|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Youanmi Terrane, Yilgarn Craton. Age dates: 2740 Ma, 2730 Ma. Consists of various unnamed metatonalites, porphyritic microgranites; metamorphosed.||||||29-SEP-11
74815|Cullculli Suite|66195|6|Mentioned|p599 Fig.2|||In the Annean Supersuite. Granitic.||||||13-MAR-12
74815|Cullculli Suite|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Mapped as five separate units, only one of which - the Cue Tonalite - is named.||Unit in Annean Supersuite.|Includes Cue Tonalite and four un-named, separately-mapped units.||Metatonalite, metagranodiorite and metatrondhjemite; typically hornblende-bearing and with common mafic clots; tonalitic gneiss, medium-grained and strongly foliated; medium- to coarse-grained leucocratic metatonalite.|
74815|Cullculli Suite|67129|5|Briefly described|p18 Fig.19, p30-34|Archean|Archean|Murchison Domain, Youanmi Terrane. Compositionally similar to Greensleeves Formation andesites: REE plot, geochemical modelling.|2785-2735 Ma|Annean Supersuite|||Mafic clotty-textured granites with REE and slight negative Eu anomaly.|06-SEP-17
74815|Cullculli Suite|68107|5|Briefly described|p618|Neoarchean|Mesoarchean|Western Youanmi Terrane.|ca. 2800-2750 Ma|Of the Annean Supersuite.|||Felsic magmatism.|
74815|Cullculli Suite|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. Foliated granodiorite gives U-Pb zircon magmatic crystallization age: 2748 +/- 3 Ma. Porphyritic microgranite  gives magmatic crystallization age: 2741 +/- 7 Ma. Metatonalite: 2733 +/- 6 Ma. From geochron files 178196.1.pdf, 185926.1.pdf, 185928.1.pdf.||Annean Supersuite|Includes Cue Tonalite and 5 unnamed units.|Co-magmatic with felsic volcanics of the Polelle Group (Murchison Supergroup)|Metatonalite, metagranodiorite, and metatrondhjemite; Tonalitic gneiss; Porphyritic microgranite; Leucocratic tonalite;|
74815|Cullculli Suite|68698|5|Briefly described|p1, p3-11, p13-19, p27-28, p33-34|Neoarchean|Neoarchean|The age range is stated (twice) as 2785-2735 Ma, despite the following age determination. Contemporaneous with the Polelle Group and Eelya Suite. A quartz diorite unit has a magmatic crystallisation age of 2746 +/- 5 Ma; a monzogranite of 2746 +/- 4 Ma; and a hornblende-biotite-quartz diorite of 2724 +/- 2 Ma (Wingate et al., 2009, 2012, 2011). Also includes a c.2787 Ma hornblende tonalite. Geochemistry is discussed in detail; the granites are interpreted to be the result of mafic-felsic magma mixing.||Annean Supersuite.||Intrudes Polelle Group.|Dominantly tonalite-trondhjemite-granodiorite, commonly containing a distinctive mafic clotty texture of elliptical (strained) hornblende +/- biotite clots to 8cm; some plutons contain synplutonic mafic dykes or mafic tonalite.|
74815|Cullculli Suite|69583|4|Described|p49, p51, p53; Plate 2|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Contemporaneous with the Polelle Group. Age range given as 2760-2735 Ma in Plate 2.|c.2785-2735 Ma.|Annean Supersuite.|Reedy Trondhjemite; Racecourse, Cue, Nannine, Snake Gully Tonalites.||Dominantly tonalite-trondhjemite-granodiorite with common distinctive mafic, clotty texture from elliptical hornblende(+ biotite) clots to 8cm; local syn-plutonic mafic dykes; local mafic tonalite with 15-20% hornblende phenocrysts.|
74815|Cullculli Suite|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean|||Annean Supersuite|Reedy Trondhjemite, Racecourse Tonalite, Cue Tonalite, Snake Gully Tonalite|||
74815|Cullculli Suite|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Annean Supersuite.|Reedy Trondhjemite; Racecourse, Cue, Snake Gully Tonalites.|||
74815|Cullculli Suite|69627|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton||Annean Supersuite|||Tonalitic gneiss; medium grained; strongly foliated.|
74815|Cullculli Suite|70020|5|Briefly described|p118,130|Neoarchean|Neoarchean|Geological province: Yilgarn Craton. TTG-like felsic intrusions.||Unit af Annean Supersuite.||Overlain by Eelya Suite. Underlain by Mount Kenneth Suite.||
74815|Cullculli Suite|70030|5|Briefly described|p190,192,205,208|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton. Mafic TTG (tonalite-trondhjemite-granodiorite) suite coeval with Polelle Group volcanism, and formation of the Hollandaire VMS deposit in the lower Greensleeves Formation.|ca. 2785-2735 Ma|Unit of Annean Supersuite.||||
74815|Cullculli Suite|70153|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Mesoarchean||2805 - 2735 Ma (inferred).|Annean Supersuite|||Metatonalite, metagranodiorite, and metatrondhjemite; typically hornblende-bearing, and with common mafic clots.|
74815|Cullculli Suite|70796|4|Described|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. Affected by the Yilgarn Craton granite magmatism (3010  2600 Ma); Youanmi Terrane events (3131  2600 Ma). See also 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 178196.1.pdf, 185926.1.pdf, 185928.1.pdf, Austin100_2442_stratig.pdf, Cue100_2443_stratig.pdf, Madoonga100_2444_stratig.pdf. Numerous additional lithologies are discussed.|2787 to 2735 Ma (inferred)|Annean Supersuite|Includes the Cue Tonalite, Racecourse Tonalite, Nannine Tonalite.|Comagmatic with the Polelle Group. Intruded by the Marlomumbah Granite.|Metatonalite, metagranodiorite, and metatrondhjemite; typically hornblendebearing, and with common mafic clots. Porphyritic microgranite, leucocratic tonalite, tonalitic gneiss.|
74815|Cullculli Suite|70826|6|Mentioned|p9|Neoarchean|Neoarchean|Youanmi Terrane.|||||Granites.|
74815|Cullculli Suite|70830|5|Briefly described|p9-p10|||Murchison Domain.||Annean Supersuite||||
74815|Cullculli Suite|71168|5|Briefly described|p7, p60|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. |c. 2780-2750 Ma|Annean Supersuite|||Granitic rocks.|
74815|Cullculli Suite|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). Sample GSWA 178196 (foliated granodiorite) yielded a concordia age of 2748+\-3 Ma, interpreted as magmatic crystallisation age. Sample GSWA 185926 (foliated porphyritic microgranite) yielded a weighted mean 207Pb/206Pb date of 2741+\-7 Ma, interpreted to be magmatic crystallization age of the microgranite. Sample GSWA 185928 (bt-hbl metatonalite) yielded a weighted mean 207Pb/206Pb date of 2733+\-6 Ma, interpreted to be igneous crystallization age of the tonaltie. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|2787-2735 Ma|Unit of Annean Supersuite.|Includes Cue Tonalite, Nannine Tonalite, Racecourse Tonalite.|In contact with, and intruded by Marlomumbah Granite pegmatites. Also crosscuts Jungar and Walganna suites.|Metatonalite, metagranodiorite, metatrondhjemite; typically hornblende-bearing, with common mafic clots; hornblende-bearing metagranodiorite with minor metatonalite; scattered small mafic xenoliths, tonalitic gneiss, porphyritic microgranite.|
74815|Cullculli Suite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma); Youanmi Terrane events (3131 - 2600 Ma). See 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|2787-2735 Ma (inferred)|Unit of Annean Supersuite.|||Metatonalite, metagranodiorite, and metatrondhjemite; typically hornblende-bearing, and with common mafic clots|
74815|Cullculli Suite|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.||Annean Supersuite.|Nannine, Racecourse Tonalites.||Tonalites.|
74815|Cullculli Suite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Youanmi Terrane.||Annean Supersuite|Includes Cue Tonalite, Nannine Tonalite.||Metatonalite, metagranodiorite, and metatrondhjemite; typically hornblende-bearing, and with common mafic clots.|
74815|Cullculli Suite|72389|5|Briefly described|Map Legend|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Gabanintha 1:100k map sheet 2644.|2785-2733 Ma|Annean Supersuite|||Metatonalite, metagranodiorite, and metatrondhjemite; typically hornblende bearing, and with common mafic clots.|28-AUG-20
74815|Cullculli Suite|73453|6|Mentioned|p2|||||||||
75509|Cullens Diamictite|64630|5|Briefly described|p31 Fig.2|Sakmarian|Gzhelian|Province: Southern Perth Basin. Underlies the Mosswood Formation. Palynology age: D. tenuistriatus. Correlates with the Shotts Formation. Inferred glacial influence.||||||24-NOV-09
75509|Cullens Diamictite|67925|6|Mentioned|Ch4 p8 fig 2|Lower Permian|Lower Permian|||Mosswood Formation||Overlain by the Woodynook Sandstone.||
75509|Cullens Diamictite|69182|6|Mentioned|Ch2 p9, Ch2 p45, Ch2 p47-p49|Early Permian|Early Permian|Perth Basin. See also Ch2 p55, Ch2 p57, Ch2 p60, Ch2 p64-p66, Ch2 p80, Ch2 p91, Ch2 p92, Ch2 p94-p96, Ch2 p98, Ch2 p100, Ch2 p102, Ch2 p104, Ch2 p106, Ch2 p108, Ch2 p110.||Stockton Group||Overlain by the Mosswood Formation.||
75509|Cullens Diamictite|70097|5|Briefly described|p19 Fig.3|Sakmarian|Asselian|Southern Perth Basin. Bunbury Trough.||Mosswood Formation||||
75509|Cullens Diamictite|71146|5|Briefly described|p6|Asselian|Asselian|Perth Basin.||||Overlain by the Mosswood Formation.|Diamictite, mudstone.|
75509|Cullens Diamictite|71377|5|Briefly described|p7|Permian|Carboniferous|Perth Basin.||Stockton Group||||
27136|Culvida Sandstone|7433|5|Briefly described|p25 Fig.2, p40-41,  p52.|Middle Triassic|Middle Triassic|Canning Basin. At least 217 m thick at BMR Cornish No. 2. Fine fluvial clastics. Excellent aquifer potential.|||||Fine quartzose sandstone, siltstone; minor redbed and greenbed units in subsurface. Plant fossils common.|
27136|Culvida Sandstone|22753|5|Briefly described|Fig.3 p585|Triassic|Triassic|||||||
27136|Culvida Sandstone|24466|5|Briefly described|p368 Fig. 3|Triassic|Triassic|||||||
27136|Culvida Sandstone|32648|6|Mentioned|p32|||Triassic||||||
27136|Culvida Sandstone|34008|6|Mentioned|p68|||Triassic||||||
27136|Culvida Sandstone|35124|6|Mentioned|Map legend|Middle Triassic|Middle Triassic|||||||
27136|Culvida Sandstone|36257|6|Mentioned|Table 2.1|||||||||
27136|Culvida Sandstone|36890|3|Fully described|p344|||||||||
27136|Culvida Sandstone|38878|6|Mentioned|Map legend|Middle Triassic|Middle Triassic|||||||
27136|Culvida Sandstone|41169|6|Mentioned|Fig.3|||||||||
27136|Culvida Sandstone|41730|6|Mentioned|Fig.3|||||||||
27136|Culvida Sandstone|43563|6|Mentioned|Fig.2,p5||Scythian|||||||
27136|Culvida Sandstone|43656|6|Mentioned|Fig.2,p8|Anisian|Scythian|||||||
27136|Culvida Sandstone|43666|6|Mentioned|p45,Table 2|Anisian|Scythian|||||||
27136|Culvida Sandstone|43746|6|Mentioned|Fig.2,p11|Anisian|Scythian|||||||
27136|Culvida Sandstone|43932|4|Described|p11,Tb.1 p5||Middle Triassic|||||||
27136|Culvida Sandstone|44143|4|Described|p.434 Table 4-19, p447|Middle Triassic|Middle Triassic|Up to 210m thick; fine to coarse sandstone; siltstone; granule and pebble conglomerate (poorly sorted); fluvial. Conformably overlies Erskine Sandstone. Type section 1km south of Culvida Soak (CORNISH: 20deg 14' 00" S, 126deg 56' 00" E). Plant fossils.||||||23-NOV-17
27136|Culvida Sandstone|44998|2|Defined|p.108-9,112-8||Triassic|Overlain probably by Godfrey Beds & Blina Shale. (F52-1). See also App.6 p295.||||||
27136|Culvida Sandstone|45153|2|Defined|App.5-90|Middle Triassic|Middle Triassic|||||||
27136|Culvida Sandstone|45158|3|Fully described|p16|||||||||
27136|Culvida Sandstone|48826|2|Defined|p.28|||Tb.III. p.28,29,30,37, Pl.1. (new name). Overlies Blina Shale or Condren Sandstone Member. May be equivalent in age to part of Erskine Sandstone. (F52-1,E52-13).||||||
27136|Culvida Sandstone|63929|6|Mentioned|p131 Fig.2.|Middle Triassic|Middle Triassic|Onshore Canning Basin.||||Overlies Erskine Sandstone.||
27136|Culvida Sandstone|66124|5|Briefly described|p169, p170 Fig.2|Anisian|Anisian|Canning Basin. Maximum 200m thick. Marine regression. Overlies Erskine Sandstone.||||||
27136|Culvida Sandstone|66949|4|Described|p26-28;p46 Appx.2;p55 Appx.3;p60 Appx.4|Middle Triassic|Middle Triassic|Type section detailed. Up to 207m thick (in BMR Cornish 2); fluvial deposits. Abundant fossil leaves. Restricted to 10km from Culvida Soak: probably a local variant of Erskine Sandstone. Available core detailed.||||?Conformably overlies and interfingers with Erskine Sandstone.|Fine- to coarse-grained sandstone; siltstone; poorly sorted granule and pebble conglomerate.|04-NOV-15
27136|Culvida Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, conglomerate, siltstone|
27136|Culvida Sandstone|72497|5|Briefly described|p3 Fig.2.|Olenekian|Induan|Shown as occuring in the Fitzroy Trough, Betty and Balgo Terraces and part of the Lennard Shelf and Margaret Terrace. Age shown as later Scythian = Induan-Olenekian.||||Conformably overlies Blina Shale.||
23525|Cunaloo Member|12471|6|Mentioned|p475 Fig.2.|Early Triassic|Early Triassic|Widespread and condensed carbonates.||Locker Shale||||24-OCT-14
23525|Cunaloo Member|13615|6|Mentioned|p6-8, p18, p42, p49|||See also p102 App. 3, p118, 119 App. 5, Plates 2,3.||Basal member of Locker Shale.|||Limestone.|07-FEB-19
23525|Cunaloo Member|40617|2|Defined|p6|Triassic|Triassic|||||||
23525|Cunaloo Member|41271|3|Fully described|p109|||||||||
23525|Cunaloo Member|41438|6|Mentioned|p106|||||||||
23525|Cunaloo Member|41440|5|Briefly described|p136|||||||||
23525|Cunaloo Member|63929|6|Mentioned|p131 Fig.2.|Early Triassic|Early Triassic|Conodont Zone: Neospathodus waageni Zone.||Unit in Locker Shale.||||
31026|Cundaline Formation|23415|5|Briefly described|Map Legend|Archean|Archean|Of Gorge Creek Group. Geological province: Pilbara Craton. Weathered brown, grey-green shale, siltstone, lithic wacke and sandstone; metamorphosed.||||||07-NOV-08
31026|Cundaline Formation|23583|5|Briefly described|Map Legend|Archean|Archean|Of Gorge Creek Group. Underlying unit Nimingarra Iron Formation. Geological Province Pilbara Craton.||||||07-NOV-08
31026|Cundaline Formation|23585|4|Described|p13|Archean|Archean|Of Gorge Creek Group. Underlain by Nimingarra Iron Formation. Geological Province: Pilbara Craton.||||||07-NOV-08
31026|Cundaline Formation|23757|4|Described|p11|Archean|Archean|Of Gorge Creek Group. Unconformably overlain by Callawa Formation; conformable on Nimingarra Iron Formation. Geological Province: Pilbara Craton. Comprises interbedded, metamorphosed, grey-green shale, siltstone and thin-bedded wacke.||||||07-NOV-08
31026|Cundaline Formation|23783|5|Briefly described|p82|||Of Gorge Creek Group.||||||
31026|Cundaline Formation|24025|4|Described|p8 Tb. 1|Archean|Archean|Of Gorge Creek Group.  Shale, siltstone, sandstone, immature pebbly sandstone and conglomerate, and wacke.  Max. thickness: ~1000m.  Geological Province: Pilbara Craton.||||||07-NOV-08
31026|Cundaline Formation|24184|5|Briefly described|p699 Fig.3|Archean|Archean|Underlying Unit: Nimingarra Formation. Geological Province: Pilbara Craton. Age:<3443Ma||||||07-NOV-08
31026|Cundaline Formation|44229|5|Briefly described|Map Legend|Archean|Archean|Of the Gorge Creek Group.  Weathered brown, grey-green shale, siltstone, lithic wacke, sandstone and pebble conglomerate.||||||07-NOV-08
31026|Cundaline Formation|50189|4|Described|p17, 25|Archean|Archean|Of the Gorge Creek Group. Comprises mixed thin to thick-bedded, red-brown weathered grey-green shale, siltstone, sandstone, immature pebbly sandstone, pebble conglomerate, and wacke. Disconformably overlies the Nimingarra Iron Formation.||||||07-NOV-08
31026|Cundaline Formation|50544|3|Fully described|p33, p19 Tb. 2 (amended)|Archean|Archean|Of the Gorge Creek Group.  Shale, siltstone, sandstone, lithic wacke, pebble conglomerate.  Disconformably overlies Nimingarra iron Formation.  Age: 3395+/-15Ma.  Max. thickness: 1000m.  See also p21 Tb. 4.||||||07-NOV-08
31026|Cundaline Formation|50555|5|Briefly described|Map legend|Archean|Archean|Of the Gorge Creek Group (Pilbara Supergroup).   Weathered-brown, grey-greenshale, siltstone, lithic wacke, sandstone, and pebble conglomerate, local polymictic, matrix-supported conglomerate.  Geological Province: Pilbara Craton.||||||07-NOV-08
31026|Cundaline Formation|60429|2|Defined|p17, p36 Appdx. 1|Archean|Archean|Disconformable on Nimingarra Iron Formation; unconform.overlain by Cooieena Basalt, Fortescue Group. + Eel Ck Fm. Age range: 3455+/-34Ma to 3395+/-15Ma. Max.thick: ~1000m. Shale, siltst., lithic wacke, sst., pebble conglomerat...further details present.||||||07-FEB-11
31026|Cundaline Formation|63441|5|Briefly described|p5 Tb.1, p26|Archean|Archean|Of Gorge Creek Group (De Grey Supergroup). Overlies Cleaverville Formation. Geological province: Gorge Creek Basin, Pilbara Craton. Consists of shale and sandstone.||||||07-FEB-11
31026|Cundaline Formation|63538|4|Described|p6 Fig. 3|Archean|Archean|Of Gorge Creek Group. Underlain by Cleaverville Formation. Geological Province: Pilbara Craton. Sedimentary rocks.||||||19-APR-13
31026|Cundaline Formation|67201|4|Described|p7 Fig.4, p12 Tb.1, p20|||East Pilbara Terrane, De Grey Superbasin, Gorge Creek Basin. In East Pilbara Terrane (p7 Fig.4); recognized only in northeast Pilbara (p20). ||Uppermost unit in Gorge Creek Group in east Pilbara||Disconformably overlies Cleaverville Formation in northeast Pilbara.|Local basal conglomerate and breccia derived from local erosion of Cleaverville Formation.|
31026|Cundaline Formation|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|Age derived from sample of quartz metasandstone (143996.1.pdf) and constrains age of deposition for sedimentary protolith.|3398 Ma +/- 15 Ma (SHRIMP)|Gorge Creek Group||Overlies Nimingarra Iron Formation|Shale, siltstone, and wacke; local sandstone and conglomerate; metamorphosed|
31026|Cundaline Formation|69301|4|Described|p5 Fig.3, p9 Tb.1, p14-15|||Pilbara Craton. East Pilbara Terrane. Gorge Creek Basin.||Top unit of Gorge Creek Group||Overlies Cleaverville Formation.|Conglomerate, sandstone and shale.|
31026|Cundaline Formation|69590|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton. Of Gorge Creek Basin, De Grey Superbasin. Events: North Pilbara Orogeny. Sample GSWA 143996 (quartzite) yielded an interpreted maximum depositional age of 3398+\-15 Ma for the sandstone protolith (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3016-3009 Ma (inferred)|Unit of Gorge Creek Group.|||Shale, siltstone, and wacke; local sandstone and conglomerate; metamorphosed|
31026|Cundaline Formation|70022|6|Mentioned|p115|||East Pilbara Terrane.||Gorge Creek Group.||||
31026|Cundaline Formation|70775|5|Briefly described|p12, p46-p47|||Gorge Creek Basin.||Gorge Creek Group||Overlies the Cleaverville Formation. Unconformably overlain by the Warambie Basalt.|Conglomerate, sandstone and shale.|
31026|Cundaline Formation|70936|6|Mentioned|p62|Archean|Archean|Geological province: Pilbara Craton.|||||Shale.|
31026|Cundaline Formation|71003|6|Mentioned|p62|Archean|Archean|Pilbara Craton. Occurs as a bedrock "island" in the Y10 pit.|||||Shale.|
31026|Cundaline Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Gorge Creek Basin.||Gorge Creek Group|||Shale, siltstone, and wacke; local sandstone and conglomerate; metamorphosed.|
31026|Cundaline Formation|72251|5|Briefly described|p54|Mesoarchean|Mesoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Gorge Creek Group.||Uppermost unit of Gorge Creek Group. Overlain by Coonieena Basalt. Underlain by Cleaverville Formation.||
31026|Cundaline Formation|72668|5|Briefly described|p4, p14|||East Pilbara Terrane.||Gorge Creek Group||Overlies the Cleaverville Formation.|Shale, conglomerate and sandstone.|
31026|Cundaline Formation|73598|6|Mentioned|p1212|Mesoarchean|Mesoarchean|East Pilbara Terrane.||Gorge Creek Group.||Overlies Cleaverville Formation. Is overlain unconformably by Coonieena Basalt.||
31772|Cundarra Granite|23569|4|Described|p6 Tb. 1|Archean|Archean|Of the Murchison Granite-Greenstone Terrane.   Coarse-grained, equigranular to porphyritic amphibolite-facies monzogranite.||||||07-NOV-08
31772|Cundarra Granite|23574|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Weiragoo Granite. Underlying unit. Tching Granite.||||||07-NOV-08
31772|Cundarra Granite|23576|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Weiragoo Granite. Underlying unit Tching Granite.||||||07-NOV-08
31772|Cundarra Granite|23577|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Weiragoo Granite. Underlying unit Tching Granite.||||||07-NOV-08
31772|Cundarra Granite|24114|5|Briefly described|p5 Fig.4|||Geological Province: Yilgarn Craton.||||||21-MAY-04
31772|Cundarra Granite|43835|5|Briefly described|Map Legend|Archean|Archean|||||||07-NOV-08
31772|Cundarra Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
31772|Cundarra Granite|71269|6|Mentioned|1m_geologyp12_lut.csv||||||||Coarse even grained to porphyritic monzogranite with amphibole, biotite or orthopyroxene clots in feldspathic halos. Retrograde amphibolite facies metamorphism.|
77800|Cundimurra Monzogranite|68287|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Shown as younger than D1 deformation (2710-2690 Ma) and older than D2 deformation (2665 - 2640 Ma). K-feldspar megacrystic biotite metamonzogranite dated by Wang, Q. (1998 ?thesis) at c. 2668 Ma.|~ 2668 Ma|Of the Tuckanarra Suite|Informally subdivided in places into three unnamed units.||Metamonzogranite to metasyenogranite; locally undeformed with common magmatic foliation (not on map); biotite metamonzogranite; K-feldspar megacrystic biotite metamonzogranite.|
77800|Cundimurra Monzogranite|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. Tuckanarra Suite not shown as 'Parent', but listed as 'Suite' for this unit.|||Includes 6 unnamed subunits.||Metamonzogranite;  monzogranite to syenogranite.|
77800|Cundimurra Monzogranite|69014|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. Geochronology by Schiotte and Campbell (1996); Wiedenbeck and Watkins (1993).|c. 2668 Ma|Of the Tuckanarra Suite.|||Biotite metamonzogranite; mylonitic; commonly with pegmatite veins and other intrusive granitic phases.|01-MAY-14
77800|Cundimurra Monzogranite|69583|5|Briefly described|p101, p113, p116-118, p121; Plate 2|Neoarchean|Neoarchean|Youanmi Terrane, Yilgarn Craton. Forms a narrow (5km x 100km), N-trending, elongate pluton. Associated with the Challa Shear Zone. Records several generations of deformation fabrics. Seismic interpretation. See also Cundimurra Granite (p45 Fig.8, p119).|c.2680-2660 Ma.|Tuckanarra Suite.|||Medium-grained, biotite-bearing monzogranite associated with tonalite and porphyritic monzogranite characterised by 2-5cm K-feldspar phenocrysts. These rocks are intruded by muscovite-(+/-garnet)-bearing leucogranite and pegmatitic to aplitic veins.|
77800|Cundimurra Monzogranite|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean|||Tuckanarra Suite|||Monzogranite.|
77800|Cundimurra Monzogranite|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain. See also Cundimurra Granite (p8 Fig.6, p16, p19, p23-27, p29, p31 Fig.33).||Tuckanarra Suite.||||
77800|Cundimurra Monzogranite|69626|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton|c.2680 Ma|Tuckanarra Suite|||K-feldspar megacrystic biotite metamonzogranite; schistose and typically with a strongly foliated, platy fabric; includes minor schlieric gneiss with well developed K-feldspar augen, sheared quartz veins, and sheared pegmatitic rocks.|
77800|Cundimurra Monzogranite|69627|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Detailed lithology in legend. |c. 2680 Ma|Tuckanarra Suite|||K-feldspar megacrystic biotite metamonzogranite; meta biotite monzogranite; fine-grained leucocratic monzogranite; equigranular monzogranite to syenogranite; K-feldspar porphyritic monzogranite to syenogranite.|
77800|Cundimurra Monzogranite|69744|6|Mentioned|p255, 259|||Syntectonic pluton. Referred to as Cundimurra pluton.||||||
77800|Cundimurra Monzogranite|70418|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|||||Equigranular, undeformed monzogranite to syenogranite; mylonitic biotite metamonzogranite commonly with pegmatite veins and other intrusive phases; K-feldspar megacrystic biotite metamonzogranite, strongly foliated.|
77800|Cundimurra Monzogranite|70770|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Three facies are mapped separately.||Tuckanarra Suite.|||K-feldspar-megacrystic biotite metamonzogranite, either strongly foliated, or schistose with minor schlieric gneiss, sheared quartz veins and pegmatitic rocks; schistose, equigranular metamonzogranite.|
77800|Cundimurra Monzogranite|70796|5|Briefly described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton. The following isotopic ages are provided: 2670 +/ 6 Ma, 2681 +/ 6 ma, 2657 +/ 9 Ma and 2680 +/ 5 Ma. Age provided from Wingate et al is interpreted as a magmatic crystallisation age. See also 100k_geologysub_lut.csv,  100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 185997.1.pdf, 198212.1.pdf, Bungar100_2539_stratig.pdf, Challa100_2541_stratig.pdf, Coolamaninu100_2540_stratig.pdf, MountMagnet100_2441_stratig.pdf, Wynyangoo100_2542_stratig.pdf.|2679 +/ 8 Ma (GSWA 185997; Wingate et al, 2015)|Tuckanarra Suite|||Schistose, equigranular metamonzogranite; includes minor schlieric gneiss, sheared quartz veins, and sheared pegmatitic rocks. Kfeldspar megacrystic biotite metamonzogranite. Biotite metamonzogranite,  leucocratic monzogranite and syenogranite.|
77800|Cundimurra Monzogranite|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma). Wingate et al., 2015 provided a crystallisation age of 2681+\-5 Ma; Wang 91998) dated a metamonzogranite at 2688+\-6 Ma. Sample GSWA 185997 (garnet-bearing aplite or microgranite gneiss) yielded a weighted mean 207Pb/206Pb date of 2679+\-8 Ma, tentatively interpreted as the magmatic crystallization age of the granite, or perhaps maximum age of granite crystallisation is the zircon age represents inheritance. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 100k_geologysub_lut.csv.|2681-2665 Ma (inferred)|Unit of Tuckanarra Suite.||Intrudes into Murchison Supergroup. Crosscut by Bald Rock Supersuite plutons.|Metamonzogranite: schistose, equigranular, k-spar megacrystic biotite, fine-grained leucocratic; syenogranite.|
77800|Cundimurra Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Includes unnamed subunit, age: 2670+/-6 Ma.|Max age 2681+/-5 ma, min 2657+/-9 Ma|Tuckanarra Suite|||Metamonzogranite to metasyenogranite; locally undeformed with common magmatic foliation. K-feldspar megacrystic biotite metamonzogranite; strongly foliated.|
40090|Curran Member|24115|5|Briefly described|p4 Fig.2|Mesoproterozoic|Mesoproterozoic|Of the Ullawarra Formation. Age: 1068 +/- 80 Ma. Geological Province: Edmund Basin.||||||
40090|Curran Member|24183|2|Defined|p17, p18|Calymmian|Statherian|Formerly known as the Curran Formation. Uppermost unit of the Ullawarra Formation. Overlain by the Coodardoo Formation. Max. Thickness: 250m. Age: 1620-1462 Ma.||||||21-MAR-11
40090|Curran Member|50292|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Geological Province: Edmund Basin.  Of the Edmund Group (Bangemall Supergroup).  Overlies Ullawarra Formation. Underlies Coodardoo Formation.||||||07-NOV-08
40090|Curran Member|50380|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Ullawarra Formation (Edmund Group). Geological Province: Edmund Basin. Has gradational contacts with underlying Ullawarra Formation and overlying Coodardoo Formation.||||||07-NOV-08
40090|Curran Member|60301|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Ullawarra Formation (Edmund Group). Geological Province: Edmund Basin. Overlies: Ullawarra Formation. Underlies: Coodardoo Formation.||||||07-NOV-08
40090|Curran Member|63471|5|Briefly described|Map legend|Mesoproterozoic||Of the Ullawarra Formation (Edmund Group, Bangemall Supergroup). Overlies the Ullawarra Formation with gradational contact. Overlain by the Coodardoo Formation with gradational contact. Geological Province: Edmund Basin. Siltstone and fine- to coarse-grained sandstone; locally intruded by dolerite sills.||||||21-MAR-11
40090|Curran Member|63869|4|Described|p37, Plate 1|Calymmian|Statherian|Formerly Curran Formation (Daniels, 1966; Chuck, 1984; Muhling and Brakel, 1985). Downgraded by Martin and Thorne (2002). Type section along eastern fork of Wannery Creek at Curran Well. 100-250 m thick. Has greater sandstone proportion than the rest of the Formation. Minimum age from dolerite sill N of Coodardoo Well (Wingate, 2002).|c.1620->1071 +/- 8 Ma.|Unit in Ullawarra Formation.||Is overlain transitionally by Coodardoo Formation.|Parallel-planar laminated siltstone interbedded with thin- to medium-bedded, fine- to coarse-grained sandstone and minor chert.|
40090|Curran Member|64728|5|Briefly described|p105.||||Maximum depositional age around 1680 +/- 8 Ma.|Unit in Ullawarra Formation.|||Interbedded fine-grained lithic sandstone and siltstone.|
40090|Curran Member|65830|4|Described|p7-8|Calymmian|Statherian|Represents a period of significantly increased siliciclastic sediment supply. Age constrained by the parent Ullawarra Formation.||Of the Ullawarra Formation||Transitionally overlain by the Coodardoo Formation.|Tabular to lenticular fine- to medium-grained sandstone beds; interbedded with minor parallel-planar-laminated siltstone.|
40090|Curran Member|69027|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Of the Ullawarra Formation.||Overlain conformably (gradationally) by the Coodardoo Formation.|Siltstone and fine- to coarse-grained sandstone; locally intruded by dolerite sills; has gradational contacts with underlying and overlying formations.|05-MAY-14
40090|Curran Member|69166|4|Described|geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Age derived from lithic sandstone sample (148974.1.pdf)|1680 Ma +/- 10 Ma(SHRIMP)|Ullawarra Formation||Overlies Ullawarra Formation, Overlain by Coodardoo Formation|Siltstone and fine- to coarse-grained sandstone; locally intruded by dolerite sills.|
40090|Curran Member|70795|4|Described|100k_geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Also 100k_interpgeop_lut.csv, 148974.1.pdf West Australian Craton, Edmund Basin|1590-1455 Ma|Ullawarra Formation||Overlies Ullawarra Formation, Conformably overlain by Coodardoo Formation|Siltstone and fine- to coarse-grained sandstone, lithic sandstone; locally intruded by dolerite sills.|
40090|Curran Member|70814|5|Briefly described|p22, p35, p57|||Edmund Basin. ||Ullawarra Formation||||04-MAY-23
40090|Curran Member|72705|5|Briefly described|p4, 9|Mesoproterozoic|Mesoproterozoic|||Ullawarra Formation.|||Turbiditic sandstone and siltstone.|
68666|Cutinduna Supersuite|63441|4|Described|p38, p12 tb. 2|Archean|Archean|Contains the Bamboo Springs Monzogranite (Shaw Granitic Complex). Age: 2905 Ma. Geological province: Pilbara Craton. See also p34 Fig. 13.||||||16-APR-13
68666|Cutinduna Supersuite|63538|6|Mentioned|p6 Fig. 3|Archean|Archean|Geological Province: Pilbara Craton.||||||19-APR-13
68666|Cutinduna Supersuite|64654|5|Briefly described|Map Legend|Archaean|Archaean|Includes Bamboo Springs Monzogranite. Age: c. 2908 Ma. Geological Province: Pilbara Craton.||||||16-APR-13
68666|Cutinduna Supersuite|64657|5|Briefly described|Map Legend|Archaean|Archaean|Includes Bamboo Springs Monzogranite. Geological Province: Pilbara Craton.||||||
68666|Cutinduna Supersuite|64728|6|Mentioned|p97.|||||Unit in Pilbara granite-greenstone terrane.||||
68666|Cutinduna Supersuite|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Pilbara Craton. c.2908 Ma. Shown as consisting of one unit, the Bamboo Springs Monzogranite.||||||
68666|Cutinduna Supersuite|66217|5|Briefly described|p9.|Mesoarchean|Mesoarchean|Granitic magmatism accompanying the accretion of the Kurrana Terrane onto the East Pilbara Terrane.|2.93-2.90 Ga.|||||
68666|Cutinduna Supersuite|67201|4|Described|p7 Fig.4, p24|||In northern Pilbara Craton, East Pilbara Terrane. Restricted to southeastern part of East Pilbara Terrane, and inliers of Kurrana Terrane within Fortescue Group.|2910-2890 Ma||||Monzogranite.|
68666|Cutinduna Supersuite|68035|5|Briefly described|p291, p286 Fig 3|Mesoarchean|Mesoarchean|SE Pilbara Craton.|2910 - 2900 Ma|||||
68666|Cutinduna Supersuite|68280|6|Mentioned|p3|Mesoarchean|Mesoarchean||2910-2900 Ma|||||
68666|Cutinduna Supersuite|68282|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|c.2908 Ma||Includes Bamboo Springs Monzogranite.|||
68666|Cutinduna Supersuite|69012|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|c.2908 Ma||Includes the Bamboo Springs Monzogranite.|||15-AUG-18
68666|Cutinduna Supersuite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean||||Includes Bamboo Springs Monzogranite|||
68666|Cutinduna Supersuite|69301|6|Mentioned|p5 Fig.3|||Pilbara Craton. East Pilbara Terrane.||||||
68666|Cutinduna Supersuite|69590|5|Briefly described|GEOL_LUT_CSV files|||Geological province: Pilbara Craton, West Australian Craton. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|||Includes Bamboo Springs Monzogranite.|||
68666|Cutinduna Supersuite|70022|6|Mentioned|p115|||East Pilbara Terrane.||||||
68666|Cutinduna Supersuite|70826|6|Mentioned|p8|Mesoarchean|Mesoarchean|||||||
68666|Cutinduna Supersuite|71550|6|Mentioned|p45|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton.|2.90-2.91 Ga|||||
68666|Cutinduna Supersuite|72251|5|Briefly described|p54|||Geological province: East Pilbara Terrane and West Pilbara Superterrane, Pilbara Craton.||||Overlain by Split Rock Supersuite. Underlain by Sisters Supersuite.||13-JAN-22
68666|Cutinduna Supersuite|72668|5|Briefly described|p4, p16-18, p29|||East Pilbara Terrane, Kurrana Terrane. Coincident with deformation across the Mosquito Creek Basin.|2910-2890 Ma||Includes Bamboo Springs Monzogranite.|||13-JAN-22
68666|Cutinduna Supersuite|73598|6|Mentioned|p1212|Mesoarchean|Mesoarchean|East Pilbara Terrane.||||||
27266|Cyril Sandstone|13194|4|Described|p393 Tb. 4-16, p402 fig 4-66|Frasnian|Frasnian|Type Section: Matheson Ridge 15o52'S 128o53'E. 180-490m thick fluvial deposits.||||Overlies Antrim Plateau Volcanics at type location. Overlain by Ragged Range Conglomerate (conformably) in Ragged Range.|Quartz sandstone and pebbly sandstone; minor conglomerate and siltstone.|
27266|Cyril Sandstone|40993|2|Defined|p4|Frasnian|Frasnian|||||||
27266|Cyril Sandstone|41864|3|Fully described|p50|||In part previously assigned to Kellys Knob Sandstone.||||||15-DEC-08
27266|Cyril Sandstone|41865|5|Briefly described|Map legend|Frasnian||||||||
27266|Cyril Sandstone|42030|5|Briefly described|p749|||||||||
27266|Cyril Sandstone|44230|5|Briefly described|Map Legend||Frasnian|||||||
27266|Cyril Sandstone|64580|6|Mentioned|map legend|||Of Cockatoo Group.||||||15-DEC-08
27266|Cyril Sandstone|69165|6|Mentioned|500k_geologyp08_lut.csv|Frasnian|Frasnian|||Cockatoo Group||||
27266|Cyril Sandstone|69452|6|Mentioned|p36:6|Frasnian|Frasnian|||Cockatoo Group.||||12-JUL-16
27266|Cyril Sandstone|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Cockatoo Group.||||
33663|Dairy Monzogranite|23786|5|Briefly described|p49|||Geological Province: Yilgarn Craton.||||||
33663|Dairy Monzogranite|44203|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
33663|Dairy Monzogranite|50075|5|Briefly described|p17|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
33663|Dairy Monzogranite|50076|5|Briefly described|Map|Archean|Archean|Biotite monzogranite.  Geological Province: Yilgarn Craton.||||||07-NOV-08
33663|Dairy Monzogranite|69152|4|Described|1m_geologyp08_lut.csv|Archean|Archean||||||Monzogranite; high-HFSE granite.|05-AUG-15
33663|Dairy Monzogranite|69631|5|Briefly described|p49|||Kookynie district.|||||Very felsic (>74% SiOs), low-Al2O3.|
33663|Dairy Monzogranite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2680 +/- 2 Ma (isotopic).||||Biotite monzogranite; metamorphosed.|
33663|Dairy Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
33663|Dairy Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 1m_geologyp12_lut.csv.|2680 Ma (inferred)||||Biotite monzogranite; metamorphosed|
28282|Dalaroo Siltstone|24160|6|Mentioned|p27 Tb. 14|Proterozoic|Proterozoic|||Billeranga Subgroup||||
28282|Dalaroo Siltstone|24410|5|Briefly described|p143 Fig. 83|Proterozoic|Proterozoic|Of the Billeranga Subgroup (Moora Group). See also p142 Tb. 60.||||||
28282|Dalaroo Siltstone|34705|6|Mentioned|p398|||||||||
28282|Dalaroo Siltstone|36293|2|Defined|p62|Proterozoic|Proterozoic|||||||
28282|Dalaroo Siltstone|36872|3|Fully described|p76|||||||||
28282|Dalaroo Siltstone|37460|6|Mentioned|p178|||||||||
28282|Dalaroo Siltstone|40307|6|Mentioned|Fig.2|||||||||
28282|Dalaroo Siltstone|40346|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
28282|Dalaroo Siltstone|40347|6|Mentioned|p16|||||||||
28282|Dalaroo Siltstone|40348|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Middle or Late||||||
28282|Dalaroo Siltstone|40349|5|Briefly described|p13|||||||||
28282|Dalaroo Siltstone|42038|6|Mentioned|p108|||||||||
23528|Dalgaranga Formation|42533|3|Fully described|p76-79|||Succession of dacite and rhyolite tuffs, volcanogenic sandstone and conglomerate, overlying the Windaning Formation||||||05-AUG-11
23528|Dalgaranga Formation|44149|5|Briefly described|p33 fig 2-29, p35 fig 2-30, p42|Archean|Archean|See also p45 Fig.2-48, p47. Of Murchison Province. About 1 km thick. Remnants of stratovolcanoes.||Mount Farmer Group||Intruded by Dalgaranga Gabbroid Complex|A sequence of dacite and rhyolite tuff, overlain by 300-400 m arkosic sandstone containing conglomerate lenses; tuff has tholeiitic affinities but the upper 200m underlying the sandstone is calc-alkaline.|
23528|Dalgaranga Formation|65268|6|Mentioned|p6 fig 4, p5 fig 3|||||Unit in Mount Farmer Group.|||Felsic volcanic and volcaniclastic rocks.|
23528|Dalgaranga Formation|69267|6|Mentioned|p654|||Murchison Province, Yilgarn Craton.||Mount Farmer Group.||||
76061|Dalgaranga dolerite|66195|5|Briefly described|p611 Fig.9|Neoarchean||See top p606. Informal reference to gabbro from Dalgaranga greenstone belt.  In the age range of the Yalgowra Suite.|Age: 2719 +/- 6 Ma.|||?intrudes the Glen Group.||13-MAR-12
76061|Dalgaranga dolerite|67129|5|Briefly described|p55|Archean|Archean|Northern Murchison Domain, Youanmi Terrane.|2719 +/- 6 Ma.|||||
76061|Dalgaranga dolerite|70020|5|Briefly described|p118|Neoarchean|Neoarchean|Geological province: Yilgarn Craton.||Unit of Yalgowra Suite.||||
76061|Dalgaranga dolerite|70830|5|Briefly described|p27-p28|||Murchison Domain.||||||
76061|Dalgaranga dolerite|71168|5|Briefly described|p7|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Yalgowra Suite||||
76061|Dalgaranga dolerite|73596|6|Mentioned|p1165, 1170|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. Presented as the formal Dalgaranga Dolerite.|2719 +/- 6 Ma.|Yalgowra Suite.||Intrudes Glen Group.||
33444|Dalgaringa Supersuite|22904|5|Briefly described|p56|||||||||16-JUL-08
33444|Dalgaringa Supersuite|23485|4|Described|p18|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
33444|Dalgaringa Supersuite|23486|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 2000-1975 Ma. Geological Province: Gascoyne Complex.||||||07-NOV-08
33444|Dalgaringa Supersuite|23487|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Complex.||||||07-NOV-08
33444|Dalgaringa Supersuite|23525|4|Described|p13|Paleoproterozoic|Archean|Consists of massive, foliated and gneissic granites.||||||07-NOV-08
33444|Dalgaringa Supersuite|23527|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Complex||||||07-NOV-08
33444|Dalgaringa Supersuite|23781|5|Briefly described|p43|Paleoproterozoic|Paleoproterozoic|Geological Province: Glenburgh Terrane.||||||07-NOV-08
33444|Dalgaringa Supersuite|24544|4|Described|p3, 27|Paleoproterozoic|Paleoproterozoic|Age: 2005-1970 Ma. Geological Province: Glenburgh Terrane of Gascoyne Complex. Massive, foliated and gneissic granites. Dominated by tonalite, diorite and granodiorite.||||||07-NOV-08
33444|Dalgaringa Supersuite|50216|5|Briefly described|p205|Paleoproterozoic|Paleoproterozoic|Proterozoic basement gneisses, granitic rocks. Age: 2005-1970 Ma. Geological Province: Glenburgh Terrane (Gascoyne Complex).||||||01-MAY-13
33444|Dalgaringa Supersuite|50218|5|Briefly described|p239, p242|Orosirian|Orosirian|Includes the Nardoo Granite. Age: 2005-1970Ma. Granitic rocks. Geological Province: Glenburgh Terrane (southern part of the Gascoyne Complex).||||||07-FEB-11
33444|Dalgaringa Supersuite|50219|4|Described|p259, p260 Fig. 2|Orosirian|Orosirian|Includes Nardoo Granite. Age 2005-1970Ma.  Geol.Prov: Glenburgh Terrane (Gascoyne Complex). See also p265.||||||07-FEB-11
33444|Dalgaringa Supersuite|50220|5|Briefly described|p280|Orosirian|Orosirian|Forms the major constituent of the Glenburgh Terrane. Age: 2005-1970 Ma.||||||
33444|Dalgaringa Supersuite|50222|5|Briefly described|p333 Tb.2, p336|Paleoproterozoic|Paleoproterozoic|Granites in the Southern Gascoyne terrane.   Age: 2.0-1.98Ma.||||||07-NOV-08
33444|Dalgaringa Supersuite|50223|5|Briefly described|p356|Paleoproterozoic|Paleoproterozoic|Age: 2005-1970Ma.  Geological Province:  Glenburgh Terrane.||||||07-NOV-08
33444|Dalgaringa Supersuite|50226|5|Briefly described|p418|Paleoproterozoic|Paleoproterozoic|Of the Gascoyne Complex (Glenburgh Terrane).  Includes foliated and gneissic granites.  Age: 2.0-1.97Ga.||||||07-NOV-08
33444|Dalgaringa Supersuite|50333|4|Described|p12|Paleoproterozoic|Paleoproterozoic|Granites.  Dominates the Glenburgh Terrane (southern part of Gascoyne Complex).  Age: 2005-1970Ma.||||||07-NOV-08
33444|Dalgaringa Supersuite|63866|4|Described|p152, p155-p157, p177|Orosirian|Orosirian|U-Pb SHRIMP zircon ages included 2003 +/- 8 Ma to 1987 +/- 4 Ma; Nelson, 1999; Kinny et al, 2004 and Sheppard et al., 2004. Glenburgh Terrane. Mistakenly referred to as the Dalaringa Supersuite on p152 and p177. Metamorphosed during the Glenburgh Orogeny.|2005-1985 Ma |||Intrudes the Halfway Gneiss and the Moogie Metamorphics. Intruded by the Nardoo Granite.|Sheets, dykes and veins of foliated and gneissic I-type tonalite, granodiorite, quartz diorite and monzogranite.|
33444|Dalgaringa Supersuite|64161|6|Mentioned|p590|Orosirian|Orosirian|Granite-dominated. Intruded during the 2005-1960 Ma Glenburgh Orogeny, Gascoyne Complex||||||
33444|Dalgaringa Supersuite|64580|4|Described|map legend||Paleoproterozoic|Granite and granitic gneiss, undivided.||||||15-DEC-08
33444|Dalgaringa Supersuite|64722|5|Briefly described|Fig. 2 p3-6, p7, 23|Orosirian|Orosirian|Magmatic arc successions overlying the Yilgarn and Pilbara cratons. Intrudes Archean gneisses of the Glenburgh Terrane.||||||11-APR-12
33444|Dalgaringa Supersuite|64728|6|Mentioned|p107.|||Southern Gascoyne Complex. Probable source of detrital zircons aged 2400-1850 Ma found in Ashburton Formation and Pooranoo Metamorphics.||||||
33444|Dalgaringa Supersuite|65152|6|Mentioned|p1.|Paleoproterozoic|Paleoproterozoic|2005 - 1970 Ma. Interpreted to have formed above a northwestward-dipping subduction zone along the southern margin of the Gascoyne Complex.||||||
33444|Dalgaringa Supersuite|65506|5|Briefly described|p995|1970 Ma.|2005 Ma.|Granitic rocks. Part of the southern Gascoyne Complex.||||||
33444|Dalgaringa Supersuite|65545|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|c. 2005 - 1970 Ma. Metagranite and granitic gneiss. See also Dalgaranga Supersuite||||||
33444|Dalgaringa Supersuite|65692|5|Briefly described|p25, p35|Orosirian|Orosirian|Intrudes the Glenburgh Terrane. Suggested source of some Earaheedy Basin sediments.|2005-1970 Ma (Sheppard et al., 2004).|||||
33444|Dalgaringa Supersuite|65830|5|Briefly described|p24, p26 Fig.13|Orosirian|Orosirian|Crystallisation ages beween 2005-1970 Ma.|2005-1970 Ma|||Intrudes the Moogie Metamorphics.|Comprises foliated and gneissic I-type tonalite, granodiorite, quartz diorite, and monzogranite, intruded by foliated mesocratic and leucocratic I-type tonalite.|
33444|Dalgaringa Supersuite|65896|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Complex. Interlayered tonalite and granodiorite, leucocratic, biotite monzogranite and granodiorite; subordinate fine-grained tonalite and monzogranite. 2005 - 1970 Ma.||||||
33444|Dalgaringa Supersuite|66299|4|Described|p1, pp71-91.|Paleoproterozoic|Paleoproterozoic|Component of southern edge of Glenburgh Terrane, basement to Gascoyne Province. Andean-type granitic batholith. Contains xenoliths from Moogie Metamorphics. Source of some components of Halfway Gneiss.|Two magma episodes: 2005-1985 Ma and c.1975 Ma.||Includes Nardoo Granite and Paradise Well diatexite.|Associated with the volcanics of Camel Hills Metamorphics. Intruded by Moorarie Supersuite granites and Bertibubba Supersuite dykes. Unconformably overlain by Lyons Group.|Foliated to gneissic granites; metatonalite and metagranodiorite; minor amphibolite, local mafic granulite. All rock types are blotchy from clots of fine-grained biotite after garnet.|
33444|Dalgaringa Supersuite|66427|5|Briefly described|p41 Tb.1, p49, p72  |||Glenburgh Terrane. Mis-spelt as Dalgaranga in Tb.1.|2005-1970 Ma (Sheppard et al., 1999).|||||
33444|Dalgaringa Supersuite|66579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, Gascoyne Province.|||Four unnamed but separately-mapped units.||Medium-grained metatonalite, metagranodiorite, biotite metamonzogranite; coarse-grained metapegmatite and metagranite; amphibolite; locally mafic granulite.|
33444|Dalgaringa Supersuite|66882|5|Briefly described|p116, p118|Orosirian|Orosirian|Southern Gascoyne Complex.|2000 Ma|||||
33444|Dalgaringa Supersuite|66887|4|Described|p1, p3 Fig.2, p5 Fig.4, p6-7, p24|Orosirian|Orosirian|Only occurs along southern margin of Glenburgh Terrane. Southern Gascoyne Province. Belt of metagranitic rocks interpreted to have formed in a continental-margin volcanic arc. In Fig.4, this unit contains the Paradise Well diatexite.|2005-1970 Ma||Nardoo Granite|In tectonic contact with Camel Hills Metamorphics. Felsic components of Dalgaringa Supersuite (c. 2000 Ma), interleave with, and have been emplaced during subduction into, Halfway Gneiss.|Metagranitic rocks. Variably deformed and metamorphosed granitic batholith. Older plutonic rocks are strongly deformed, and locally contain decametre-scale strips and lenses of  granulite-facies pelitic diatexite.|14-DEC-16
33444|Dalgaringa Supersuite|66950|5|Briefly described|p7, p9 Fig.8, p10 Fig.9, pp13-15|Orosirian|Orosirian||c. 2005-1970 Ma|||Intrudes the Halfway Gneiss and Moogie Metamorphics.|Comprises foliated to gneissic granites.|
33444|Dalgaringa Supersuite|67247|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, Gascoyne Province. Also includes four un-named sub-units mapped separately.|2002 - 1974 Ma.||Includes Nardoo Granite.||Metagranite and granitic gneiss.|
33444|Dalgaringa Supersuite|67371|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, Gascoyne Province. Also includes 8 separately-mapped but un-named units.|2002 - 1974 Ma.||Includes Nardoo Granite.||Biotite metatonalite and meta quartz diorite; foliated biotite metamonzogranite; mesocratic metatonalite; foliated metagranodiorite and metamonzogranite sheets with abundant mafic granulite; metapegmatite and metagranite; amphibolite.|
33444|Dalgaringa Supersuite|67843|3|Fully described|Throughout the article.|Paleoproterozoic|Paleoproterozoic|Intermediate to felsic plutonic rocks with Andean-type subduction zone geochemical and isotopic characteristics. Deformation and mineralogy are described in detail.|2005-1985 Ma.||Includes Nardoo Granite.|Is intruded by Nardoo Granite.|Foliated, strongly layered metatonalites, metagranodiorites and metamonzogranites.|
33444|Dalgaringa Supersuite|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic||||||granite and granitic gneiss|
33444|Dalgaringa Supersuite|68981|5|Briefly described|p1, p17 Fig.4, p19-20, p22-23|||Glenburgh Terrane. Hf evolution diagrams. Origin of inherited zircons discussed.|2005-1970 Ma.||||Includes an arc-related granitic batholith.|
33444|Dalgaringa Supersuite|69003|5|Briefly described|p4, p9-10|||Glenburgh Terrane, Capricorn Orogen. Continental-margin arc setting.|2005-1970 Ma.||||Felsic granitic gneisses, pelitic schists and granites.|
33444|Dalgaringa Supersuite|69028|5|Briefly described|Map Legend|Orosirian|Orosirian|Glenburgh Terrane, Gascoyne Province.|2005-1985 Ma||||Metagranite and granitic gneiss.|06-MAY-14
33444|Dalgaringa Supersuite|69080|5|Briefly described|p684, p688-689, p694 Fig.9, p696|Orosirian|Orosirian|Glenburgh Terrane, Gascoyne Province. Formed in a supra-subduction zone setting; represents the exhumed mid-crustal portions of a continental-margin arc known as the Dalgaringa Arc.|2005-1975 Ma.||Includes Nardoo Granite.||Metagranite and granitic gneiss.|
33444|Dalgaringa Supersuite|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic||||Includes Nardoo Granite||Metagranite, granitic gneiss, leucocratic biotite metamonzogranite and metagranodiorite, leucocratic metapegmatite and metagranite, metatonalite, leucocratic metatonalite, amphibolite, mafic granulite, minor pelite, diatexite migmatite.|
33444|Dalgaringa Supersuite|69237|6|Mentioned|p2|Orosirian|Orosirian|Gascoyne Province.|2005-1970 Ma.|||||
33444|Dalgaringa Supersuite|69387|4|Described|p3, p6, p12, p14, p21-22, p26-29, p35|Orosirian|Orosirian|See also p37, p40, p68. Glenburgh Terrane, Gascoyne Province. An extensive granite batholith, formed in a continental margin arc. Deformations discussed. SG and magnetic susceptibility values given. Gravity and magnetic modelling. Hosts base metal and gold mineralisation.|2002-1975 Ma.||Nardoo Granite.|Intrudes Halfway Gneiss and Moogie Metamorphics.|Granitic rocks and gneisses. I-type (Na-rich).|
33444|Dalgaringa Supersuite|69546|5|Briefly described|p102|Orosirian|Rhyacian|Geological province: Gascoyne Province.|2005-1970 Ma|||||
33444|Dalgaringa Supersuite|69583|5|Briefly described|p130-132, p137, Plate 3|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Formed in a continent-margin volcanic arc. Age-range also given as c.2005-1970 Ma.|c.2005-1985 Ma.||||Metagranitic rocks:  massive, foliated, and gneissic granitic rocks; lenses of pelitic diatexite and mafic granulite.|
33444|Dalgaringa Supersuite|69596|5|Briefly described|p5-6, p9|Orosirian|Rhyacian|Glenburgh Terrane, Gascoyne Province. Continental margin arc setting.|c.2000 Ma.|||Intrudes Halfway Gneiss and Moogie Metamorphics.|Extensive granite batholith.|
33444|Dalgaringa Supersuite|70019|5|Briefly described|p94|Orosirian|Orosirian|Geological province: Gascoyne Province, Capricorn Orogen. Comprises Neoarchean to Paleoproterozoic basement rock assemblage of the Gascoyne Province.|2005-1970 Ma|||||
33444|Dalgaringa Supersuite|70090|6|Mentioned|p453|Orosirian|Orosirian|Continental magmatic arc; formed on the southern margin of the Glenburgh Terrane during the Glenburgh Orogeny, prior to collision with the northern Yilgarn Craton (Sheppard et al., 2004; Johnsonet al., 2011b). Intruded into basement to the Gelnburgh Terrane.|2005-1970 Ma|||||
33444|Dalgaringa Supersuite|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 2_5m_interpgeop15_lut.csv, 100k_geologyl_lut.csv, 100k_geologysub_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, West Australian Craton|2002-1974 Ma|||Intruded by Scrubber Granite, Moorarie Supersuite|Medium grained, leucocratic biotite metamonzogranite, leucocratic metapegmatite, granitic gneiss, metagranite, mesocratic metatonalite, amphibolite, locally granulite. Foliated metagranodiorite and metamonzogranite sheets.|
33444|Dalgaringa Supersuite|70796|4|Described|2_5m_interpgeop15_lut.csv|Paleoproterozoic|Paleoproterozoic|Of the Capricorn Orogen, Gascoyne Province, Glenburgh Terrane. Affected by the following events: Edmundian Orogeny (1026  954 Ma); Capricorn Orogeny (1817  1772 Ma); Glenburgh Orogeny D2 (1966  1947 Ma); Glenburgh Orogeny (2002  1947 Ma); Glenburgh Orogeny D1 (2002  1987 Ma). See also 500k_interpgeop_lut.csv.|2002 +/ 5 Ma to 1974 +/ 4 Ma (isotopic)||||Metagranite and granitic gneiss|
33444|Dalgaringa Supersuite|70814|6|Mentioned|p4, p35 fig 19, p60|||||||||
33444|Dalgaringa Supersuite|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|Southern Gascoyne Province.||||Intrudes the Camel Hills Metamorphics.||
33444|Dalgaringa Supersuite|71000|5|Briefly described|p64, 66-67, 70|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, southern Gascoyne Province, Capricorn Orogen. Voluminous arc magmatism intrusions. Hosts the Glenburgh Au deposit. Trace element (LA-ICPMS) analyses tabulated. Geochemistry, mineralogy, geochronology all discussed in  detail. Photomicrographs.|2005-1975 Ma.|||Intrudes Halfway Gneiss. Faulted against (in tectonic contact with) Camel Hills Metamorphics.|Calc-alkaline intrusions; biotite metamonzogranite, metatonalite, metagranodiorite, amphibolite, locally mafic granulite.|
33444|Dalgaringa Supersuite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||acid intrusive rock|
33444|Dalgaringa Supersuite|71269|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Gascoyne Province, Glenburgh Terrane, Capricorn Orogen, West Australian Craton. Events: Edmundian Orogeny (1026-954 Ma); Capricorn Orogeny (1817-1772 Ma); Glenburgh Orogeny D2 (1966-1947 Ma); Glenburgh Orogeny (2002-1947 Ma); Glenburgh Orogeny D1 (2002-1987 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv.|2002+\-5 Ma; 1974+\-4 Ma (isotopic)||||Metagranite and granitic gneiss|
33444|Dalgaringa Supersuite|71468|5|Briefly described|p26,38|Orosirian|Orosirian|Geological province: Gacoyne Province. "Andean-type" batholith associated with continental-margin arc magmatic activity (the Dalgaringa Arc). Comprises granitic gneisses that have major and trace element signatures that are consistent with formation in a suprasubduction zone setting (Sheppard et al., 2004).|2005-1970 Ma|||||
33444|Dalgaringa Supersuite|71804|6|Mentioned|p403 fig 10|||Gascoyne Province.||||||
33444|Dalgaringa Supersuite|71869|5|Briefly described|p2-p4, p9, p11-p14, p17-p18, app p3-p4|||Glenburgh Terrane, Capricorn Orogen. Forms an extensive batholith along the southern margin of the Glenburgh Terrane. Geochemistry suggests generation in a continental margin arc setting.|2005-1975 Ma||Includes the Nardoo Granite.||Intermediate to granitic rocks including tonalite, granodiorite, monzogranite, leucocratic pegmatite and granulite.|17-AUG-22
33444|Dalgaringa Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, Capricorn Orogen.|Max age 2002+/-5 Ma, min 1974+/-4 Ma.||||Metagranite and granitic gneiss.|
33444|Dalgaringa Supersuite|72259|6|Mentioned|p3-4, p6, App. Tb.B|Orosirian|Orosirian|[Age range written as ca. 2005-1945 Ma and ca. 2005-1970 Ma]. [Article examines the age and geochemistry of rutile from this unit].|ca. 2005-1945 Ma||||Includes pelitic schist and biotite tonalite.|
33444|Dalgaringa Supersuite|72705|6|Mentioned|p3|||Western Australian Craton. Arc-related; associated with the Glenburgh Orogeny.|2005 - 1970 Ma.|||||
33444|Dalgaringa Supersuite|73102|5|Briefly described|p3|||Gascoyne Province; Glenburgh Terrane.|||||Metagranite and granitic gneiss.|
33444|Dalgaringa Supersuite|73168|6|Mentioned|p758, p765|Orosirian|Orosirian|Gascoyne Province, Glenburgh Terrane.|2005-1970 Ma||Nardoo Granite|||
33444|Dalgaringa Supersuite|73214|5|Briefly described|p974 Fig.1|Palaeoproterozoic||Glenburgh Terrane.|||Nardoo Granite.|||
33444|Dalgaringa Supersuite|73442|5|Briefly described|p3|||Gascoyne Province, Glenburgh Terrane.|||||Metagranite and granitic gneiss.|
32238|Dalton Suite|23416|5|Briefly described|Map Legend|Archean|Archean|In the Pilbara Craton||||||07-NOV-08
32238|Dalton Suite|23755|4|Described|p45|Archean|Archean|Of Gorge Creek Group?||||||07-NOV-08
32238|Dalton Suite|23783|6|Mentioned|p17|||||||||
32238|Dalton Suite|24025|4|Described|p8 Tb. 1|Archean|Archean|Layered mafic and ultramafic sills intruding Gorge Creek and Sulphur Springs Groups and Strelley Granite.  Age: c.3070Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
32238|Dalton Suite|24110|5|Briefly described|Plate 1|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
32238|Dalton Suite|24184|5|Briefly described|p702, 703|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
32238|Dalton Suite|24531|4|Described|p20|Archean|Archean|Mafic and ultramafic sills that lie within the Gorge Creek and Sulphur Springs Groups, and in the Euro Basalt.  See also p8-9 Fig. 3. Geological Province: Pilbara Craton.||||||07-NOV-08
32238|Dalton Suite|24532|5|Briefly described|Map legend|Archean|Archean|Of the Pilbara Supergroup.||||||07-NOV-08
32238|Dalton Suite|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Of the Gorge Creek Group - layered ultramafic-mafic sills within the Soanesville Subgroup.||||||07-FEB-11
32238|Dalton Suite|61253|5|Briefly described| p52 Fig. 2|Archean|Archean|Age: ?3070Ma. Geological Province: eastern Pilbara Craton. See also p54-55 Fig. 3.||||||07-NOV-08
32238|Dalton Suite|61266|5|Briefly described|p58 Tb.1, p60|Archean|Archean|Of the Gorge Creek Group. Age: <3235 Ma. A series of differentiated ultramafic to mafic sills. Occur primarily within the Paddy Market Formation, locally within the Corboy Formation and large sill intrudes the Strelley Granite. Geol. Prov: Pilbara Craton||||||07-NOV-08
32238|Dalton Suite|63417|5|Briefly described|Map legend|Archean|Archean|Of the Pilbara Supergroup. Geological Province: Pilbara Craton. Mafic and ultramafic intrusive rocks; metamorphosed.||||||07-NOV-08
32238|Dalton Suite|63441|5|Briefly described|p13 tb. 2|Archean|Archean|Age: 3200Ma. Geological province: Pilbara Craton. See also p32 Fig. 11.||||||07-FEB-11
32238|Dalton Suite|63538|6|Mentioned|p6 Fig. 3|Archean|Archean|Geological Province: Pilbara Craton.||||||19-APR-13
32238|Dalton Suite|64580|4|Described|map legend||Mesoarchean|Undivided; mafic and ultramafic intrusive rocks; metamorphosed.||||||15-DEC-08
32238|Dalton Suite|64621|5|Briefly described|Map legend|Archean|Archean|Rocks laid down at time of c.3180Ma Rifting event. Metadunite (schistose); metaperidote and serpentine-chlorite schist; schistose serpentinite and metaleucogabbro. No named constituents included.||||||07-NOV-08
32238|Dalton Suite|65727|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|East Pilbara Terrane, Pilbara Craton.|c.3180 Ma.|Of Pilbara Supergroup (PROBABLE MAP LEGEND ERROR)|||Metaperidotite and serpentine-chlorite schist; carbonate-tremolite-chlorite rock.|22-MAR-13
32238|Dalton Suite|65827|4|Described|p28, p46|||Composed of layered ultramafic-mafic sills. Intrudes Euro Basalt, Panorama Formation, Wyman Formation. Includes large serpentinised peridotite bodies, metapyroxenite; hosts quantities of high-grade chrysotile fibre.||||||
32238|Dalton Suite|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Pilbara Craton. Age shown as c.3185 Ma. Metamorphosed mafic and ultramafic intrusive rocks.||||||
32238|Dalton Suite|66118|4|Described|p147-149 Fig.3, p155, p156 Fig.11|||Pilbara Craton. Interpreted as subvolcanic sills to the Honeyeater Basalt. Age interpreted as igneous emplacement age of sill as well as eruptive age of associated Honeyeater Basalt (Soanesville Group).|3182+/-2 Ma SHRIMP U-Pb zircon|||Intrudes Honeyeater Basalt. Intrudes Paddy Market Formation, Corboy Formation and Pincunah Hill Formation in Soanesville greenstone belt.|Subvolcanic sills: layered mafic-ultramafic and range in composition from dunite, through pyroxenite, to dolerite and local granophyre at the top of some sills.|
32238|Dalton Suite|66217|5|Briefly described|p10, p38.|||Emplacement possibly due to rifting associated with Soanesville Event at 3200-3165 Ma. Hosts PGE and Ni mineralisation.|||||Layered ultramafic-mafic intrusions.|
32238|Dalton Suite|67201|4|Described|p7 Fig.4, p19, p26|Archean|Archean|East Pilbara Terrane.|c. 3180 Ma|Mount Billroth Supersuite|||Ultramafic and mafic sills.|
32238|Dalton Suite|67269|5|Briefly described|p5|Paleoarchean|Paleoarchean|||Gorge Creek Group.|||Mafic and ultramafic intrusive rocks.|
32238|Dalton Suite|68035|5|Briefly described|p289, 285, 291, 294|Mesoarchean|Mesoarchean|May intrude northern boundary of Kurrana Terrane as mafic and ultramafic sills. Contain Ni-Cu mineralisation, but grades are generally <1% Ni.|3180 Ma|||Intruded East Pilbara Terrane, Soanesville Basin units and other rifted margin units.|Dolerite, gabbro, and ultramafic rocks. Rift-related.|23-MAY-16
32238|Dalton Suite|68282|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|Pilbara Craton. 7 facies are mapped separately.|c.3185 Ma||||Partly serpentinized dunite and peridotite; pyroxenite; pyroxene leucogabbro; gabbro and dolerite with local diorite; all metamorphosed; metaperidotite and serpentine-chlorite schist; tectonic megabreccia with talc-chlorite-carbonate matrix.|
32238|Dalton Suite|68284|5|Briefly described|p6-7, 9|Archean|Archean|Kelly greenstone belt, East Pilbara Terrane.|3182 Ma (Van Kranendonk et al., 2010).|||Intrudes Kelly Group.|Metaperidotite: carbonate-tremolite schist; metaperidotite: serpentine-chlorite schist.|
32238|Dalton Suite|69012|5|Briefly described|Map Legend|Mesoarchean||Soanesville Basin. Nine facies are mapped separately.|< c. 3185||||Pyroxene-hornblende metagabbro; metadolerite and local mafic schist; metadunite; schistose metadunite; metaperidotite and serpentine-chlorite schist; schistose serpentinite; metapyroxenite; metaleucogabbro; metadolerite.|28-APR-14
32238|Dalton Suite|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Soanesville Basin. Includes 4 unnamed facies mapped separately.|c. 3185 Ma||||Comprises schistose meta-ultramafic rock intruded by granite rock; meta-ultramafic intrusive rock; serpentinite, schistose; metadolerite.|29-APR-14
32238|Dalton Suite|69015|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton. Age from a dolerite and mafic schist unit. See map legend for a detailed lithological description. Mapped as 11 unnamed sub-units.|c. 3185 Ma.||||Metaperidotite and serpentine-chlorite schist; serpentinite; metadolerite; metagabbro; gabbro and dolerite; pyroxene leucogabbro; dolerite; pyroxenite; peridotite; dunite.|02-MAY-14
32238|Dalton Suite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean||||||Megabreccia, metadunite metaperidotite and serpentine schist, serpentinite. Metapyroxenite, metadolerite, metagabbro and metaleucogabbro. Dunite and peridotite; partly serpentinized and metamorphosed. Gabbro, dolerite; metamorphosed.|
32238|Dalton Suite|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|||Includes Shay Intrusion.||Undivided; mafic and ultramafic intrusive rocks; metamorphosed|
32238|Dalton Suite|69301|4|Described|p5 Fig.3, p12-13|||Pilbara Craton. East Pilbara Terrane.|3.18 Ga, Van Kranendonk et al. 2006a|||Intrudes Soanesville Group. Intrudes Kurrana Shear Zone (boundary between the Kurrana Terrane and the Mosquito Creek Basin).|Ultramafic and mafic sills.|
32238|Dalton Suite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Of Soanesville Basin. Events: Mosquito Creek Orogeny; North Pilbara Orogeny; Prinsep Orogeny; East Pilbara Terrane Rifting Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv.|3185 Ma (isotopic, inferred)|||Intrudes into Kangaroo Caves Formation.|(Meta)dolerite, (meta)dunite, (meta)gabbro, (meta)peridotite, pyroxenite, serpentinite, tectonic megabreccia, tectonically interleaved ultramafic schist and ultramafic intrusive rocks; carbonate altered, metamorphosed.|
32238|Dalton Suite|69616|5|Briefly described|p159-166, p171-177, p180-184|||Maximum thickness of 200m. Very rare sulfides, restricted to dolerite.||Unit in Mount Billroth Supersuite.||Intrudes Paddy Market Formation.|Differentiated mafic and ultramafic sills, commonly dolerite overlying basal pyroxenite and dunite.|
32238|Dalton Suite|70022|6|Mentioned|p115|||East Pilbara Terrane.||||||
32238|Dalton Suite|70826|6|Mentioned|p8|Mesoarchean|Mesoarchean|East Pilbara Terrane.|||||Mafic and ultramafic intrusive rocks.|
32238|Dalton Suite|71041|6|Mentioned|p45 fig 2|||||||Intrudes the Kangaroo Caves Formation, Corboy Formation and the Honeyeater Basalt.|Ultramafics.|
32238|Dalton Suite|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||dolerite, gabbro, dunite, peridotite, serpentinite|
32238|Dalton Suite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Soanesville Basin.|3185+/-2 Ma.||One unamed sub-unit.||Mafic and ultramafic intrusive rocks; metamorphosed. Metamorphosed ultramafic intrusive rock.|
32238|Dalton Suite|72251|6|Mentioned|p55|||Of Shaw Granitic Complex.||||||
34108|Daltons Creek Granite|22615|5|Briefly described|p 8||Archean|SHRIMP 2936+/- 5Ma||||||07-NOV-08
30537|Dalyup Gneiss|22448|6|Mentioned|p877 Fig.3||Statherian|||||||
30537|Dalyup Gneiss|24165|5|Briefly described|Plate 1|Mesoproterozoic|Mesoproterozoic|||Biranup Complex.|||Granitic augen gneiss and granitoid gneiss.|
30537|Dalyup Gneiss|24526|5|Briefly described|p105 Fig. 6, p107|Mesoproterozoic|Mesoproterozoic|Of the Biranup Complex; exotic to the Yilgarn Craton. Comprises biotite-hornblende granodiorite and monzogranite gneiss. Interleaved with metagabbro and pyroxene granulite of the Fraser Complex.  Age: 1650-1300Ma. See also p106 Fig. 7, p112 Fig. 9.||||||15-DEC-08
30537|Dalyup Gneiss|43203|5|Briefly described|Map Legend||Proterozoic|Biranup Complex||||||
30537|Dalyup Gneiss|43212|6|Mentioned|p7|||U-Pb SHRIMP of this complex formed at c.1700-2630 Ma.||||||
30537|Dalyup Gneiss|43280|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Albany-Fraser Orogen||||||
30537|Dalyup Gneiss|43498|4|Described|4||Proterozoic|U-Pb ages: 1600-1700Ma.||||||15-DEC-08
30537|Dalyup Gneiss|43838|5|Briefly described|p3, 8||Proterozoic|In Albany-Fraser Orogen||||||12-JUL-16
30537|Dalyup Gneiss|62093|5|Briefly described|p217|Paleoproterozoic|Paleoproterozoic|Age: 1700-1600Ma. Geological Province: at boundary between Biranup Complex and Yilgarn Craton.||||||07-NOV-08
30537|Dalyup Gneiss|62381|4|Described|p2 Fig.2, p3 Fig.3, p6|||Exotic to the Yilgarn Craton.|1695-1634 Ma.|Unit in Biranup Complex.||Intruded by 1300-1280 Ma granite and granodiorite.|Biotite-hornblende granodiorite and monzogranite gneiss.|30-JUN-14
30537|Dalyup Gneiss|63866|4|Described|p183, p185, p188-p189, p191, p198|Statherian|Statherian|Biranup Complex. Extends from Bremer bay area to inboard of the Fraser Comnplexand forms the main suture to the craton margin. Precise SHRIMP protolith crystallization dates from Nelson et al, 1996 are: 1670 +/- 15 Ma, 1671 +/- 16 Ma, 1634 +/- 26 Ma, 1692 +/- 22 Ma, 1695 +/- 16 Ma. Additional SHRIMP ages from Spaggiari et al, 2007 include 1680 +/- 7 Ma and 1689 +/- 11 Ma. Metamorphic zircon growth was timed at 1197 +/- 12 Ma.|1695-1634 Ma (Nelson et al., 1995)||||Biotite-hornblende granodiorite and monzogranite gneiss.|
30537|Dalyup Gneiss|64577|5|Briefly described|p606 Fig. 1, p607, p608 Fig. 2, p616-617|||Of Biranup Complex. Age: 1700-1630Ma.||||||
30537|Dalyup Gneiss|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Granitic augen gneiss and granitic gneiss.||||||15-DEC-08
30537|Dalyup Gneiss|64722|5|Briefly described|Fig. 2 p3-6, p18|Statherian|Statherian|Part of the Biranup Complex of the Albany-Fraser Orogen. Intruded by 1300-1280 Ma granitic rocks. Components of this unit make up the Corumup Gneiss.|Protolith age of 1700-1630 Ma.||||Felsic orthogneiss.|11-APR-12
30537|Dalyup Gneiss|65257|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Granitic gneiss.||||||16-JUN-09
30537|Dalyup Gneiss|65260|6|Mentioned|p8 Fig.3, p16|Statherian|Statherian|Part of Biranup Complex. Granitic gneiss; in places interleaved with Archean rocks. U-Pb zircon age of 1670+/-15 Ma (Nelson et al. 1995).||||||
30537|Dalyup Gneiss|65487|3|Fully described|p2-3 Figs.1-2, p24, p27-43, p50, p54-61|||Main component of the Biranup Zone. Granitic protoliths 1690-1660 Ma; intensely deformed and metamorphosed up to granulite facies. Metamorphism ~1180 Ma.Granodioritic, monzogranitic, syenogranitic gneisses, OPX-bearing granitic gneiss, and quartz-magnetite gneiss, mafic gneiss and amphibolite; strongly magnetic - distinctly linear trending. Deformation and geochronology described in great detail.||||||10-FEB-14
30537|Dalyup Gneiss|67268|5|Briefly described|p6, p7, p9|Paleoproterozoic|Paleoproterozoic|Similar to the Coramup Gneiss in age and lithology. Biranup Zone. Age of granitic protolith approximately 1680 ma (SHRIMP, Nelson et al 1995)|1690-1660 Ma (Bodorkos & Clark 2004)|||Intruded by the Recherche Supersuite|Granitic gneisses, granodiorite, monzogranite, syenogranite and minor mafics.|15-JUN-22
30537|Dalyup Gneiss|67323|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Albany-Fraser Belt, along the Yilgarn Craton margin. Plate margin magmatism.|~1690-1670 Ma.||||Felsic and mafic granulites, felsic gneiss, gabbro and metagabbro, amphibolite, microgranite and pegmatite.|
30537|Dalyup Gneiss|67581|6|Mentioned|p44 Fig.8|||||||||
30537|Dalyup Gneiss|67722|5|Briefly described|p5 fig 2.2, p8-10, p17|Paleoproterozoic|Paleoproterozoic|Main component Biranup Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen. |crystallisation ages 1695-1634 Ma (SHRIMP)||||Includes biotite-hornblende granodiorite, monzogranite gneiss, metafelsic and metamafic rocks.|
30537|Dalyup Gneiss|68186|6|Mentioned|p19|||Myers (1995) included this unit in the Biranup Complex.||||||
30537|Dalyup Gneiss|69152|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic||||||Granitic gneiss; heterogeneous; includes mafic phases.|05-AUG-15
30537|Dalyup Gneiss|69252|5|Briefly described|p13-14|||Biranup Zone (formerly the Biranup Complex), Kepa Kurl Booya Province.|||||Orthogneisses and metagabbros.|
30537|Dalyup Gneiss|69559|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Granitic augen gneiss and granitic gneiss.|
30537|Dalyup Gneiss|70085|6|Mentioned|p234 Fig.1|||Biranup Zone, Albany-Fraser Orogeny.||||||
30537|Dalyup Gneiss|70153|5|Briefly described|100k_geologyp10_lut.csv|Mesoproterozoic|Paleoproterozoic||||||Mafic gneiss, metagabbro, mafic granulites; orthopyroxene rich. Felsic granulites, some with garnets. Subordinate metagranitic rocks.|
30537|Dalyup Gneiss|70802|5|Briefly described|100k_geologyp10_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Kepa Kurl Booya Province, Albany-Fraser Orogen.|||||Granitic gneiss; heterogeneous; includes mafic phases|
30537|Dalyup Gneiss|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||felsic gneiss|
30537|Dalyup Gneiss|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Biranup Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen. See 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|||||Granitic gneiss; heterogeneous; includes mafic phases|
30537|Dalyup Gneiss|72491|6|Mentioned|p2|Calymmian|Calymmian|||||||
39347|Danjo Monzogranite|24091|4|Described|p66|Archean|Archean|Age: 2703+/-4Ma (Pb/Pb). Geological Province: Yilgarn Craton.||||||07-NOV-08
39347|Danjo Monzogranite|24196|5|Briefly described|p45|Archean|Archean|Age: 2703 +/- 4 Ma (U-Pb: Fletcher et al., 2001). Geological Provnce: Yilgarn Craton||||||07-NOV-08
68658|Dardie Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Foliated porphyritic monzogranite; microcline porphyroclasts.|05-AUG-15
68658|Dardie Monzogranite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||3010 - 2600 Ma (inferred).||||Porphyritic monzogranite; microcline porphyroclasts; locally foliated; metamorphosed.|
68658|Dardie Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
68658|Dardie Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|3010-2600 Ma (inferred)||||Porphyritic monzogranite; microcline porphyroclasts; locally foliated; metamorphosed|
23532|Darkan Quartz Monzonite|39160|4|Described|p44|||Analysis geochemistry||||||19-DEC-06
23532|Darkan Quartz Monzonite|40359|4|Described|p10|||||||||
23532|Darkan Quartz Monzonite|40370|6|Mentioned|p10|||||||||
23532|Darkan Quartz Monzonite|42396|6|Mentioned|p2|||||||||
23532|Darkan Quartz Monzonite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite, monzogranite, diorite, quartz monzonite|
25872|Darlot Formation|41199|2|Defined|p20|late Quaternary||Reserved as Darlot||||||
25872|Darlot Formation|43065|6|Mentioned|p93|||||||||
77788|Dave Hill intrusion|60498|5|Briefly described|p1019-1020.|Paleoproterozoic|Paleoproterozoic|No lithology was stated for the stratigraphic name. Electron microprobe geochemical analyses of apatites and biotites are detailed.|||||Includes olivine gabbronorite.|
77788|Dave Hill intrusion|71873|5|Briefly described|p426-431,433-434,437-441,444|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province. U-Pb detrital zircon magmatic age includes 1839+\-6 Ma. Cut by a mafic-diorite dyke that yields U-Pb age of 1829+\-3 Ma.||Unit of Sally Malay Suite.|||Mafic-ultramafic cumulates include olivine-rich troctolites to olivine leuco-norites with prominent orthopyroxene oikocrysts.|
73607|Davey Well Granite|63469|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Of Durlacher Supersuite. Consists of schistose coarse-grained, strongly porphyritic biotite metamonzogranite; rounded phenocrysts of K-feldspar up to 6cm in diameter.||||||24-JUN-13
73607|Davey Well Granite|63470|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Durlacher Supersuite. Geological Province: Gascoyne Complex. Schistose, fine- and medium-grained biotite monzogranite, sparsely to moderately porphyritic.||||||07-NOV-08
73607|Davey Well Granite|66299|4|Described|p247-251, p193-194, p277-286.|Paleoproterozoic|Paleoproterozoic|Oval to round K-feldspar phenocrysts up to 6cm diameter. Consists probably of multiple intrusive events spanning several million years. Forms what Williams (1986) referred to as the (informal) Yinnetharra Gneiss Dome. Main gneissic fabric is related to Mutherbukin Tectonic Event (1280-1250 Ma).|1667 +/- 4 Ma to 1648 +/- 6 Ma. |Unit in Durlacher Supersuite.|Encloses Tetlow Granite.|Is faulted against schists of Leake Spring Metamorphics. Intrudes  Moorarie Supersuite. Intrudes, and has faulted contacts with, Halfway Gneiss. Extensively intruded by Mundine Well Dolerite Suite.|Strongly-foliated, coarse-grained biotite metamonzogranite with prominent K-feldspar phenocrysts.|22-NOV-13
73607|Davey Well Granite|67373|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.||Unit in Durlacher Supersuite.|||Schistose, coarse-grained, strongly porphyritic biotite metamonzogranite with round phenocrysts of K-feldspar to 6 cm diameter; local mesocratic biotite metamonzogranite with tabular K-feldspar phenocrysts to 3 cm diameter.|
73607|Davey Well Granite|68521|5|Briefly described|Map Legend|Statherian|Statherian|Geochronology from Sheppard et al. (2005).|c.1680-1620 Ma|Of the Durlacher Supersuite.|||Schistose, coarse-grained, strongly porphyritic biotite metamonzogranite; round phenocrysts of K-feldspar up to 6 cm in diameter.|
73607|Davey Well Granite|68522|5|Briefly described|Map Legend|Statherian|Statherian|Gascoyne Province. Geochronology from Sheppard et al.(2005).|1680-1620 Ma|Of the Durlacher Supersuite.|||Schistose, coarse-grained, strongly porphyritic biotite metamonzogranite; round phenocrysts of K-feldspar up to 6 cm in diameter.|
73607|Davey Well Granite|69011|5|Briefly described|Map Legend|Statherian|Statherian|Gascoyne Province.||Of the Durlacher Supersuite.|||Comprises schistose, coarse-grained, strongly porphyritic biotite metamonzogranite; round phenocrysts of K-feldspar up to 6 cm in diameter.|
73607|Davey Well Granite|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Age derived from metamonzogranite samples (183215.1.pdf, 185944.1.pdf) Previously known as Yinnetharra Gneiss Dome.|1653  +/- 10Ma, 1667  +/- 3 Ma(SHRIMP)|Durlacher Supersuite|||Schistose, coarse-grained, strongly porphyritic biotite metamonzogranite and coarse grained, porphyritic mesocratic biotite metamonzogranite.|
73607|Davey Well Granite|70127|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|1682-1619 Ma.|Durlacher Supersuite.|||Schistose, coarse-grained, strongly porphyritic biotite metamonzogranite; round phenocrysts of K-feldspar up to 6cm in diameter.|
73607|Davey Well Granite|70138|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.||Durlacher Supersuite.|||Schistose, coarse-grained, strongly porphyritic biotite metamonzogranite; round phenocrysts of K-feldspar up to 6cm in diameter.|
73607|Davey Well Granite|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 183207.1.pdf, 183215.1.pdf, 185944.1.pdf, 195819.1.pdf, 195826.1.pdf|1680-1620 Ma|Durlacher Supersuite||Intruded by Thirty Three Supersuite|Schistose, coarse grained, strongly porphyritic biotite metamonzogranite, mica-tourmaline metamonzogranite, coarse grained porphyritic mesocratic biotite metamonzogranite.|
73607|Davey Well Granite|70814|6|Mentioned|p67-p68|||||||||
73607|Davey Well Granite|71869|5|Briefly described|p8, app p16-p17|||Capricorn Orogen.|1653 +/- 10 Ma, 1667 +/- 4 Ma (cryst. Age)|Durlacher Supersuite|||Porphyritic monzogranite, coarse-grained porphyritic biotite monzogranite.|17-AUG-22
39506|Davitt Syenogranite|63417|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite.  Geological Province: Pilbara Craton. Muscovite-garnet syenogranite; medium-grained; foliated; metamorphosed.||||||07-NOV-08
39506|Davitt Syenogranite|63441|5|Briefly described|p8 Tb. 2|Archean|Archean|Of Emu Pool Supersuite. Geological province: Pilbara Craton.||||||07-FEB-11
39506|Davitt Syenogranite|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||Of Mount Edgar Granitoid Complex.|||Muscovite-garnet syenogranite, medium-grained, foliated.|
39506|Davitt Syenogranite|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of Emu Pool Supersuite.|||Muscovite-garnet syenogranite, medium-grained, foliated, metamorphosed.|
39506|Davitt Syenogranite|65827|2|Defined|p6 Tb.2, p9 Fig 3, p23, p58|Paleoarchean|Paleoarchean|New name; 8km long and 600m wide lenticular body near Davitt Well. >3315 Ma. Foliated, inequigranular, medium-grained, leucocratic, pink-grey muscovite-garnet syenogranite. Intrudes Fig Tree Gneiss; intruded by Kennell Granodiorite. Of Emu Pool Supersuite.||||||
39506|Davitt Syenogranite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Emu Pool Supersuite|||Muscovite--garnet syenogranite; medium grained, foliated; weakly metamorphosed|
39506|Davitt Syenogranite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3325-3277 Ma (inferred)|Unit of Emu Pool Supersuite.|||Muscovite-garnet syenogranite; medium grained, foliated; weakly metamorphosed|
39506|Davitt Syenogranite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|||Emu Pool Supersuite|||Muscovite--garnet syenogranite; medium grained, foliated; weakly metamorphosed.|
79347|Davyhurst Granite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|3010-2600 Ma (inferred)||||Granite; typically poorly exposed and deeply weathered|
78637|Day Rock Granodiorite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Granodiorite; metamorphosed.|05-AUG-15
78637|Day Rock Granodiorite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|See also 500k_interpgeop14_lut.csv.|2676 +/- 5 Ma (isotopic).||||Granodiorite; metamorphosed.|
78637|Day Rock Granodiorite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv.|2676+\-5 Ma||||Granodiorite; metamorphosed|
78637|Day Rock Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||2676+/-5 Ma||||Granodiorite; metamorphosed.|
38805|Daylight Well Granodiorite|23930|5|Briefly described|p131|Archean|Archean|Geological Province: Yilgarn Craton. Age: 2658+/-6Ma.||||||07-NOV-08
38805|Daylight Well Granodiorite|60981|5|Briefly described|p175 Fig.1|Archean|Archean|Age: 2666+/- 6 Ma.||||||07-NOV-08
69685|De Grey Supergroup|61253|5|Briefly described| p53|Archean|Archean|Supersedes De Grey Group. Comprises Croydon, Bookingarra, Goldsworthy and Nullagine Groups. Occurs in the Mosquito Creek Basin, Mallina Basin and Lalla Rookh Basin (Pilbara Craton). See also p50 Fig. 1, p52 Fig. 2.||||||07-NOV-08
69685|De Grey Supergroup|61264|5|Briefly described|p62|Archean|Archean|Supersedes the De Grey Group. Includes the Nullagine Group. Age: 2970-2920Ma. Geological Province: northen Pilbara Craton and Mallina Basin.||||||07-NOV-08
69685|De Grey Supergroup|63245|5|Briefly described|p4 Fig. 1|Archean|Archean|Age: c.2940Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
69685|De Grey Supergroup|63417|5|Briefly described|Map legend|Archean|Archean|Includes Gorge Creek and Nullagine Groups.  Age range: c. 3020 to <2950Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
69685|De Grey Supergroup|63420|5|Briefly described|Map legend|Archean|Archean|Includes the Gorge Creek and Croydon Groups. Ages included: c.3020Ma, c.2948Ma and c.2912Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
69685|De Grey Supergroup|63441|4|Described|p5 Tb. 1, p14 Fig. 2. p24-25|Archean|Archean|Supersedes De Grey Group (Hickman 1990). Redefined to include Croydon, Nullagine,Whim Creek and Gorge Creek Groups. Age: c.3.02-2.93Ga. Mostly clastic sedimentary rocks/lesser volcanic rocks deposited in five basins constituting the De Grey Superbasin.||||||07-FEB-11
69685|De Grey Supergroup|63538|4|Described|p2 Fig. 1, p5, p7, p11, p18|Archean|Archean|Age: 3020-2930 Ma. Includes Croydon and Nullagine Groups and Bookingarra Formation. Geological Province: Pilbara Craton. Clastic sedimentary rocks, chert, banded iron-formation, and minor felsic volcaniclastic rocks.||||||17-APR-13
69685|De Grey Supergroup|63649|5|Briefly described|p200 Fig. 1|Archean|Archean|Geological Province: West Pilbara Terrane/ Regal Terrane in the De Grey Superbasin.||||||07-FEB-11
69685|De Grey Supergroup|63854|5|Briefly described|p228, p229 Fig.2, p230  |Mesoarchean|Mesoarchean|Pilbara Craton.|ca. 3020-2920 Ma||Includes Nullagine Group, Mosquito Creek Formation, Lalla Rookh Sandstone, Mallina and Paradise Formations.|||
69685|De Grey Supergroup|64174|5|Briefly described|Map legend|Archean|Archean|Includes the Croydon and Whim Creek Groups. Age range: c.2964Ma - 2943Ma. Geological province: Mallina Basin.||||||07-NOV-08
69685|De Grey Supergroup|64405|5|Briefly described|p2 Fig. 1, p4 Fig. 3|Archean|Archean|Geological province: De Grey Superbasin.||||||07-FEB-11
69685|De Grey Supergroup|64580|4|Described|map legend||Mesoarchean|Siliciclastic sedimentary rocks; metamorphosed.||||||22-OCT-08
69685|De Grey Supergroup|64621|5|Briefly described|Map legend|Archean|Archean|Includes the Gorge Creek and Croydon Groups.  Age: c.3020Ma.||||||07-NOV-08
69685|De Grey Supergroup|64632|5|Briefly described|p202-203, p200, p205, 207|Mesoarchean|Mesoarchean||3020-2930 Ma||Gorge Creek Group, Whim Creek Group, Croydon Group, Nullagine Group, each deposited in separate basins.||Composed of predominantly coarse clastic rocks.|
69685|De Grey Supergroup|64654|5|Briefly described|Map Legend|Archaean|Archaean|Includes Nullagine Group. Geological Province: Pilbara Craton.||||||17-NOV-08
69685|De Grey Supergroup|64747|6|Mentioned|p94 fig 1, p95 fig 2|Mesoarchean|Mesoarchean||c.2940 Ma.|||||
69685|De Grey Supergroup|65727|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Gorge Creek Basin, Pilbara Craton.|||Includes Gorge Creek Group.|||
69685|De Grey Supergroup|65825|5|Briefly described|p5, pp31-32.|Archean|Archean|Redefined (Van Kranendonk et al. 2004) De Grey Group.|c.2.97 - 2.92 Ga.||Includes Nullagine Group.|||
69685|De Grey Supergroup|65827|5|Briefly described|p3 Fig.1, p6 Tb.1, p8|Mesoarchean|Mesoarchean|Northern Pilbara Craton. 3.02-2.93 Ga. Includes Gorge Creek Group; includes Cleaverville Formation. Unconformably overlies Pilbara Supergroup. Predominantly sedimentary rocks.||||||21-JAN-22
69685|De Grey Supergroup|65829|6|Mentioned|p2 Fig.1. |||||||||
69685|De Grey Supergroup|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|De Grey Superbasin, Pilbara Craton. Includes Gorge Creek Group and Croydon Group.||||||
69685|De Grey Supergroup|66118|4|Described|p146-148, p151, p153 Fig.7, p159-160|||Pilbara Craton. Deposited across the whole of the Pilbara Craton.|3020-2930 Ma||Croydon Group, Nullagine Group, Whim Creek Group, Gorge Creek Group, Cleaverville Formation|Unconformably overlies West Pilbara Superterrane, East Pilbara Terrane and Kurrana Terrane rocks.|Dominantly clastic sediments|
69685|De Grey Supergroup|66122|5|Briefly described|p74|Archean|Archean||3.02 - 2.93 Ga.||Gorge Creek Group.|Unconformably overlies Pilbara Supergroup.||
69685|De Grey Supergroup|66217|4|Described|pp1-2, p5, p6 Table 1, p9, p12, pp39-43|Mesoarchean|Mesoarchean|East Pilbara Terrane, Pilbara Craton. Low-grade metasedimentary rocks. Deposited after the Prinsep Orogeny of c.3.07-3.05 Ga. Thickness varies up to 8000 m.|3020-2930 Ma.||Includes Gorge Creek, Whim Creek, Nullagine and Croydon Groups.|Overlies unconformably the Warrawoona Group (Pilbara Supergroup) and Muccan Granitic Complex. Is unconformably overlain by Mount Bruce Supergroup.|Dominantly clastic sedimentary rocks, banded iron-formation and chert; subordinate mafic and felsic volcanic rocks.|
69685|De Grey Supergroup|66664|6|Mentioned|p3.  |||Fortescue Basin.||||||
69685|De Grey Supergroup|66745|5|Briefly described|p50 Fig.1, p53 Fig. 3.|Mesoarchean|Mesoarchean||||Includes Croydon Group and Mosquito Creek Formation.|Unconformably overlies Soanesville Group.|Coarse clastic rocks.|12-OCT-15
69685|De Grey Supergroup|67130|5|Briefly described|p13, p61, p62|Mesoarchean|Mesoarchean|Deposited over rocks of the West Pilbara Superterrane, East Pilbara Superterrane and the Kurrana Terrane.|3020 Ma - 2930 Ma||Gorge Creek Group, Whim Creek Group, Croydon Group, Nullagine Group. Includes Cleaverville Formation|Unconformably overlies Pilbara Supergroup, overlies Gorge Creek Group|Clastic sedimentary rocks.|
69685|De Grey Supergroup|67197|5|Briefly described|p3, p5, p9, p14, p19, p22, p25, p29|||See also p33-34, p36, p38. De Grey Superbasin.|c.3020-2930 Ma.||Gorge Creek, Gordon Groups.|Unconformably overlies Soanesville Group.||
69685|De Grey Supergroup|67201|4|Described|p3, p7-10, p12, p16-17 Fig.9, p20, p64|Archean|Archean|In northwestern Pilbara Craton, De Grey Superbasin, West Pilbara Superterrane. Detrital zircons: 3795 Ma Constantine Sandstone (Nelson 2000); 3714 Ma Mosquito Creek Formation (Nelson 2005).|||Gorge Creek Group (at base), Croydon Group, Whim Creek Group, Nullagine Group.|||05-DEC-16
69685|De Grey Supergroup|67269|6|Mentioned|p2 Fig.1|Paleoarchean|Paleoarchean|De Grey Superbasin.||||||
69685|De Grey Supergroup|67270|6|Mentioned|p3|||De Grey Superbasin.||||||
69685|De Grey Supergroup|67668|6|Mentioned|p. 154; Figs. 1-2;||Mesoarchean|East Pilbara Terrane, Pilbara Craton.|3020 - 2930 Ma||Gorge Creek Group.|Unconformably overlies the Pilbara Supergroup.||
69685|De Grey Supergroup|68035|6|Mentioned|p289, p285 Fig 2|Mesoarchean|Mesoarchean|De Grey Superbasin.||||||
69685|De Grey Supergroup|68280|6|Mentioned|p1, p19||||c. 2940 Ma|||||13-JAN-23
69685|De Grey Supergroup|68281|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|De Grey Superbasin, Pilbara Craton. Age inferred from ages of prior (Prinsep) and closing (North Pilbara) Orogenies.|3070-2950 Ma.||Includes Croydon Group, Gorge Creek Group.|||02-DEC-14
69685|De Grey Supergroup|68282|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|De Grey Superbasin.|||Includes the Croydon Group.|||03-DEC-14
69685|De Grey Supergroup|68283|5|Briefly described|Map Legend|Mesoarchean|Paleoarchean|Gorge Creek, Mallina and Lalla Rookh Basins.|< 3235 Ma||Includes Croydon Group, Gorge Creek Group.|||
69685|De Grey Supergroup|68284|5|Briefly described|p2|||De Grey Superbasin, East Pilbara Terrane.||||||
69685|De Grey Supergroup|69012|5|Briefly described|Map Legend|Archean|Archean|De Grey Superbasin.|||Includes Gorge Creek Group.|||
69685|De Grey Supergroup|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|De Grey Superbasin.|||Includes the Croydon Group and the Gorge Creek Group.|||
69685|De Grey Supergroup|69015|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|De Grey Superbasin.|||Includes the Croydon Group and the Gorge Creek Group.|||
69685|De Grey Supergroup|69167|6|Mentioned|geologyp_lut.csv|Mesoarchean|Mesoarchean||||Includes Croydon Group, Nullagine Group, Gorge Creek Group|||
69685|De Grey Supergroup|69185|4|Described|GEOL_LUT_CSV files|||Geological Province: Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|||Includes Croydon Group, Gorge Creek Group, Nullagine Group; Cattle Well Formation, Cooragoora Formation.||Siliciclastic sedimentary rocks; metamorphosed|
69685|De Grey Supergroup|69301|4|Described|p3-5, p9 Tb.1, p21 Fig.8, p22|||Pilbara Craton. De Grey Superbasin. Detrital zircons in De Grey Supergroup include 3.80 Ga zircon (Mallina Basin, Nelson 2000) and 3.71 Ga zircon (Mosquito Creek Basin, Nelson 2005).|3050-2930 Ma||Croydon Group, Whim Creek Group, Gorge Creek Group, Nullagine Group|Is overlain by Mount Bruce Supergroup with regional unconformity. Overlies Soanesville Greoup with regional unconformity.||
69685|De Grey Supergroup|69548|6|Mentioned|p2|||Pilbara region.|||||Mostly sedimentary rocks.|
69685|De Grey Supergroup|69590|5|Briefly described|GEOL_LUT_CSV files|||Geological province: Pilbara Craton. Of De Grey Superbasin. See 250k_interpgeop_lut.csv, 100k_geologyp_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeol_lut.csv.|||Includes Croydon Group, Gorge Creek Group, Nullagine Group, Paradse Plains Formation.|||
69685|De Grey Supergroup|69616|5|Briefly described|p160-161|Archean|Archean|Unconformably overlies basement in north Pilbara Craton. Maximum depositional age of c.3020 Ma (Van Kranendonk et al., 2006).|3.02-2.92 Ga.|||||
69685|De Grey Supergroup|70022|6|Mentioned|p113, 115|||Pilbara Craton. Associated with an extensional period following amalgamation of the East Pilbara Terrane and the West Pilbara Superterrane.|3.05 - 2.93 Ga.||Croydon, Whim Creek, Gorge Creek, Nullagine Groups.||Sedimentary and volcanic rocks.|
69685|De Grey Supergroup|70507|6|Mentioned|p431|Archean|Archean|Geological province: Pilbara Craton.||||||
69685|De Grey Supergroup|70729|6|Mentioned|p164|||Geological province: East Pilbara Terrane, Pilbara Craton. Of De Grey Superbasin.||||||
69685|De Grey Supergroup|70733|6|Mentioned|p105|||Eastern Pilbara Craton.||||||
69685|De Grey Supergroup|70775|5|Briefly described|p6, p13, p15, p38-p39, p95|Archean|Archean|De Grey Superbasin.|||Includes the Gorge Creek Group, Whim Creek Group and the Bookingarra Group.|||
69685|De Grey Supergroup|70826|6|Mentioned|p6 tbl 2, p8|Mesoarchean|Mesoarchean|De Grey Superbasin.||||||
69685|De Grey Supergroup|70834|6|Mentioned|p298|||Marble Bar greenstone belt, Pilbara Craton.||||||
69685|De Grey Supergroup|70884|6|Mentioned|p122|Mesoarchean|Mesoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|3.05-2.93 Ga|||||
69685|De Grey Supergroup|71041|6|Mentioned|p42||||3050-2930 Ma.|||||
69685|De Grey Supergroup|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||shale, greywacke, sandstone, banded iron formation|
69685|De Grey Supergroup|71487|5|Briefly described|p128|Archean|Archean|Of De Grey Superbasin.||||Overlain by Fortescue Group. Underlain by Soanesville Group.||
69685|De Grey Supergroup|72034|6|Mentioned|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Coonieena Basalt, Gorge Creek Group.|||
69685|De Grey Supergroup|72064|5|Briefly described|p65-66|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawoona Group.||||
69685|De Grey Supergroup|72251|5|Briefly described|p53-54|Mesoarchean|Mesoarchean|Geological province: East Pilbara Terrane and West Pilbara Superterrane, Pilbara Craton. Volcanic and sedimentary sequence deposited during an extensional event, after amalgamation of the East Pilbara Terrane and West Pilbara Superterrane.|3.06-2.93 Ga||Includes Bookingarra, Whim Creek, Croydon and Gorge Creek groups.|||
69685|De Grey Supergroup|72668|4|Described|p2, p3-5, p11-15, p21, p24-25, p28|||Dominates the West Pilbara Superterrane and the Karratha Terrane. Recently redefined to include four groups deposited in five basins. Geochemistry is discussed.|ca. 3020-2930 Ma||Includes the Whim Creek Group, Gorge Creek Group, Nullagine Group and Croydon Group.|Intruded by the Orpheus Supersuite and the Maitland River Supersuite.|Primarily coarse clastic rocks.|13-JAN-22
69685|De Grey Supergroup|73160|6|Mentioned|p2 Fig.1|||||||Unconformably overlies Kelly Group, unconformably underlies Fortescue Group.||
69685|De Grey Supergroup|73598|6|Mentioned|p1212|Mesoarchean|Mesoarchean||||Gorge Creek, Croydon Groups.|Unconformably overlies Pilbara Supergroup.||
35396|Dead Bullock Formation|23809|5|Briefly described|p3-4|||Siltstone, graphitic shale, iron-rich beds and silicified nodular chert.  Overlain conformably by Killi Killi Formation.  Max. thickness: 4km.||||||
35396|Dead Bullock Formation|50152|5|Briefly described|p71, p72 Fig. 3|||Of Tanami Group. Conformably underlian by Killi Killi Formation. Comprises graphitic siltstones, mudstones, silicatefacies banded iron formations, cherts and dolerite sills.||||||
35396|Dead Bullock Formation|50315|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group. Siltstone: white, dark grey to black, thin bedded mudstone, siltstone and black carbonaceous shale, includes minor banded iron formation, thin pale calcareous beds and thin bedded chert; chert nodules common.||||||07-NOV-08
35396|Dead Bullock Formation|50374|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tanami Group||||||07-NOV-08
35396|Dead Bullock Formation|50376|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tanami Group. Siltstone; siltstone and black carbonaceous shale, includes minor banded iron formation, thin plae calcareous beds and thin bedded chert; chert nodules common.||||||07-NOV-08
35396|Dead Bullock Formation|60676|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Tanami Group. Underlies: Killi Killi Formation. Overlies: MacFarlane Peak Group. Siltstone: thin bedded mudstone, siltstone and carbonaceous shale, includes banded iron formation, thin calcareous beds, thin bedded chert; chert nodules, dolerite sills.||||||07-NOV-08
35396|Dead Bullock Formation|60681|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Tanami Group. Siltstone, numerous dolerite sills.||||||
35396|Dead Bullock Formation|61861|3|Fully described|p10-12, p3, 4, p9, Figs.11-15,  Map 1|Orosirian|Orosirian|New name. Includes former Mount Charles Beds. Hosts significant gold mineralisation. Forms small isolated silicified outcrops. Intruded by numerous granite bodies, dolerite dykes and sills.Correlated with Halls Creek and Pine Creek Orogen units.|1880-1850 Ma on basis of correlations.|Unit in Tanami Group.||Overlies MacFarlane Peak Group (or possibly laterally equivalent). Is overlain by Killi Killi Formation, transitionally in places. May be lateral equivalent to Twigg Formation.|A succession dominated by fine-grained sedimentary rocks: buff, grey or purple siltstone with interbedded black carbonaceous siltstone or shale, calc-silicates, thin bedded chert and banded iron formation; minor thin-bedded quartz rich sandstone.|
35396|Dead Bullock Formation|62377|4|Described|p1, 11-15|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group. Sandstone, siltstone, schist, iron formation and mafic rocks. Underlies Killi Killi Formation conformably. Unconformably overlain by Pargee Sandstone, Muriel Range Sandstone, Lucas Formation and Pedestal beds. Max age: 1865 +/- 12Ma (youngest detrital zircon grain).||||||10-DEC-12
35396|Dead Bullock Formation|62580|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group.||||||07-FEB-11
35396|Dead Bullock Formation|62628|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group. Geological Province: Tanami Inlier.||||||07-NOV-08
35396|Dead Bullock Formation|62632|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group. Geological Province: Tanami/Arunta Region-Aileron Province. Grey siltstone, silty shale, fine grained sandstone, laminated siltstone, massive quartzite, black shale, chert, amphibolite.||||||07-NOV-08
35396|Dead Bullock Formation|62637|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group. Geological Province: Tanami/Arunta Region - Aileron Province. Grey siltstone, intercalated chert, interbedded silty shale, fine grained sandstone, laminated siltstone, massive quartzite, black shale.||||||07-NOV-08
35396|Dead Bullock Formation|63261|3|Fully described|p9 Fig. 5, p10-11|Paleoproterozoic|Paleoproterozoic|Of Tanami Gp. Contains lower Ferdies Member + overlying Callie Member.Conformably overlain by Killi Killi Fm. Fining-upward, deep water succession dominated by siltstone, carbonaceous siltstone, Fe-rich siltstone+mafic sills. Geol.prov: Tanami Region.||||||07-FEB-11
35396|Dead Bullock Formation|63866|5|Briefly described|p92|||Tanami Region.|c. 1840 Ma|||Overlain by the Killi Killi Formation.|Tuff.|
35396|Dead Bullock Formation|64662|5|Briefly described|p28, 27|Orosirian|Rhyacian|Basal unit of Tanami Group. Age of deposition (inferred): ~2.11-1.84Ga. Underlies Killi Killi Fm. Comprises lower sst/upper carbonaceous siltst. Detrital zircons derived from Archean basement, not contemporaneous orogenic products.||||||07-FEB-11
35396|Dead Bullock Formation|64675|5|Briefly described|p9, p10, Maps1, 6, p20, Fig.30-32|Paleoproterozoic|Paleoproterozoic|||Of the Tanami Group.||Underlain by the MacFarlane Peak Group. Overlain by the Killi Killi Formation.|Comprises a siltstone unit with minor carbonaceous shale, calc-silicate and banded iron formation.|19-MAR-14
35396|Dead Bullock Formation|64725|5|Briefly described|p62.|||Host rock for most of the gold in the Granites-Tanami Orogen.|c.1847-1840 Ma.|Lower unit in Tanami Group.|||Carbonaceous siltstone and iron-formation; extensively hydrothermally altered.|
35396|Dead Bullock Formation|64733|3|Fully described|p170 Fig.2, p171-172, p172 Fig.4, p182|Orosirian|Orosirian|1km thick.  Suggested back-arc basin or volcanic arc tectonic setting at time of deposition. Age from tuffaceous sandstone (Cross and Crispe, 2007).|SHRIMP U-Pb zircon age of 1838 +/- 6 Ma.|Of Tanami Group.|Lower part of the Formation is called the Ferdies Member. Upper part  - Callie Member.|Overlain by Killi Killi Formation; overlies Stubbins Formation. Intruded by Inspiration Peak Granite.|Upward-fining sequence of sandstone, turbiditic sandstone, carbonaceous siltstone, siltstone, shale, chert and rare volcanics.|20-APR-12
35396|Dead Bullock Formation|64734|4|Described|p187, p191, p199, p201-2, p186 Fig.1|Orosirian||Basal Tanami Group; includes Ferdies Member, Callie Member; fine sst, siltst (some carbonaceous) grade into chert-bearing BIF and clayst; base unseen; deposited ~1838Ma; large gold deposits; conformable boundary with Killi Killi Formation above suggested||||||10-FEB-11
35396|Dead Bullock Formation|64735|6|Mentioned|p217||||||Includes Callie Member.|||30-APR-12
35396|Dead Bullock Formation|64737|5|Briefly described|p233||Orosirian|Age from a volcaniclastic unit.|1838+/-6 Ma (Cross and Crispe, 2007).|||Overlain by Killi Killi Formation.||01-MAY-12
35396|Dead Bullock Formation|64956|6|Mentioned|p11|||||||||07-FEB-11
35396|Dead Bullock Formation|65323|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Tanami Group; siltstone with numerous moderate-highly magnetic metadolerite sills; moderate-intensely magnetic with a high gravity response; underlies Killi Killi Formation||||||02-FEB-10
35396|Dead Bullock Formation|65324|5|Briefly described|Map legend|Orosirian|Orosirian|Of Tanami Group; underlies Killi Killi Formation. White, dark grey-black, thin bedded mudst, siltst, black carbonaceous shales; minor BIF, thin calcareous beds and thin bedded chert; chert nodules common; contains many metadolerite sills ||||||
35396|Dead Bullock Formation|65326|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Tanami Group; siltstone with numerous moderate-highly magnetic metadolerite sills; moderate-intensely magnetic with a high gravity response; underlies Killi Killi Formation||||||02-FEB-10
35396|Dead Bullock Formation|65327|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Tanami Group; siltstone with numerous moderate-highly magnetic metadolerite sills; moderate-intensely magnetic with a high gravity response; underlies Killi Killi Formation||||||
35396|Dead Bullock Formation|65328|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Tanami Group; siltstone with numerous moderate-highly magnetic metadolerite sills; moderate-intensely magnetic with a high gravity response; underlies Killi Killi Formation||||||02-FEB-10
35396|Dead Bullock Formation|65349|5|Briefly described|Map legend|Orosirian|Orosirian|Of Tanami Group; underlies Killi Killi Formation. White, dark grey-black, thin bedded mudst, siltst, black carbonaceous shales; minor banded iron formation, thin calcareous beds, thin bedded chert; chert nodules common; contains many metadolerite sills||||||
35396|Dead Bullock Formation|65350|5|Briefly described|Map legend|Orosirian|Orosirian|Of Tanami Group; underlies Killi Killi Formation. White, dark grey-black, thin bedded mudst, siltst, black carbonaceous shales; minor banded iron formation, thin calcareous beds, thin bedded chert; chert nodules common; contains many metadolerite sills||||||02-MAR-10
35396|Dead Bullock Formation|65351|5|Briefly described|Map legend|Orosirian|Orosirian|Of Tanami Group; underlies Killi Killi Formation. White, dark grey-black, thin bedded mudst, siltst, black carbonaceous shales; minor banded iron formation, thin calcareous beds, thin bedded chert; chert nodules common; contains many metadolerite sills||||||02-MAR-10
35396|Dead Bullock Formation|65352|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Tanami Group; Siltstone with numerous moderate-highly magnetic metadolerite sills; moderate-intensely magnetic with a high gravity response; underlies Killi Killi Formation||||||02-FEB-10
35396|Dead Bullock Formation|65353|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Tanami Group; Siltstone with numerous moderate-highly magnetic metadolerite sills; moderate-intensely magnetic with a high gravity response; underlies Killi Killi Formation||||||02-FEB-10
35396|Dead Bullock Formation|65354|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Tanami Group; siltstone with numerous moderate-highly magnetic metadolerite sills; moderate-intensely magnetic with a high gravity response; underlies Killi Killi Formation||||||
35396|Dead Bullock Formation|65355|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map; of the Tanami Group||||||
35396|Dead Bullock Formation|65356|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map; of the Tanami Group; underlies Killi Killi Formation||||||
35396|Dead Bullock Formation|65358|4|Described|p6|Orosirian|Orosirian|In Tanami Region. Basal unit of Tanami Group. Conformably overlain by Killi Killi Formation. Upward-fining deep water succession dominated by siltstone, carbonaceous siltstone, banded iron formation and mafic sills. Carbonaceous- and iron-rich lithologies are important hosts for gold mineralisation.||||||
35396|Dead Bullock Formation|66129|4|Described|p213, p214 Fig.1, p216 Fig.3|Orosirian|Orosirian|1864-1844 Ma. ~1km thick, upward fining sequence of metasedimentary sandstone, siltstone, shale, chert and rare volcanics. Contains Callie and Ferdies Members. Unit in Tanami Group. Unconformably overlies Billabong Complex.||||||30-MAR-15
35396|Dead Bullock Formation|66468|5|Briefly described|p16-17, p19|Orosirian|Orosirian|~1864-1844 Ma. ~1km thick. Sandstone, iron-rich siltstone, carbonaceous shale, chert, pillow basalt and rare volcanic rocks. Unconformably overlies Billabong Complex. Conformably underlies Killi Killi Formation. Includes Ferdies and Callie Members.||||||
35396|Dead Bullock Formation|67163|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.||Unit in Tanami Group.||Is overlain by Killi Killi Formation.|Grey siltstone, silty shale, fine-grained sandstone, laminated siltstone, massive quartzite, fine-grained black shale, chert, boudin chert, amphibolite.|20-OCT-11
35396|Dead Bullock Formation|67165|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province.||Unit in Tanami Group.||Overlain by Killi Killi Formation.|Grey siltstone, silty shale, fine-grained sandstone, laminated siltstone, massive quartzite, fine-grained black shale, chert, boudin chert, amphibolite.|20-OCT-11
35396|Dead Bullock Formation|67168|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lateral equivalent of lower part of Twigg Formation.||Unit in Tanami Group.||Is overlain by Killi Killi Formation.|Siltstone, numerous metadolerite sills.|
35396|Dead Bullock Formation|67824|4|Described|p383-396|Orosirian|Orosirian|Hosts gold, particularly where crustal faults intersect claystone facies.|~ 1840 Ma|Of the Tanami Group.|Includes Ferdies Member, Callie Member.|Is overlain by Killi Killi Formation.|Contains mafic sediment that is iron-rich.|
35396|Dead Bullock Formation|67826|4|Described|p401 Fig.2, p402|Orosirian|Orosirian|207Pb/206Pb zircon age from a tuff. Lower part of the Tanami Group stratigraphy.|~ 1838 +/- 6 Ma|Of the Tanami Group.|Includes Callie Member, Ferdies Member|Is overlain conformably by Killi Killi Formation.|Consists of graphitic and iron-rich sandstones and siltstones.|
35396|Dead Bullock Formation|68474|4|Described|p572, p574|||Granites-Tanami Orogen. See also Dead Bullock Group. 1km thick. Interpreted to be derived from a provenance dominated by a bimodal suite of Archaean mafic and felsic rocks.||Tanami Group|Includes the Callie Member and the Ferdies Member.|Conformably overlain by the Killi Killi Formation.|Sandstone, turbiditic sandstone, carbonaceous siltstone, siltstone, shale, chert and rare volcanic rocks.|
35396|Dead Bullock Formation|68656|6|Mentioned|GEOCHRON|Paleoproterozoic|Paleoproterozoic|||Tanami Group||Is overlain conformably by Killi Killi Formation.||
35396|Dead Bullock Formation|69003|4|Described|p16-17|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. Deformed by the c.1844-c.1825 Ma Tanami Event and the c.1795 Ma Tanami Orogeny.|1847-1840 Ma.|Tanami Group.||Unconformably overlies the Billabong Complex. Is overlain unconformably by Killi Killi Formation. Lateral equivalent of Stubbins Formation.|Siliciclastic metasedimentary rocks.|
35396|Dead Bullock Formation|69253|4|Described|p746, p747 Fig.1, p748, p753-767|Orosirian|Orosirian|Redefined to include the Stubbins and Mount Charles Formations in WA. ~3 km thick. Predominantly back-arc affinity. Petrophysical properties detailed.|c.1864 Ma (Bagas et al., 2008).|Unit in Tanami Group.||Is intruded by Lewis and Selby Granites. Is overlain conformably by Killi Killi Formation.|Succession of turbiditic sandstone, variably ferruginous and carbonaceous shale, chert, basalt, and associated dolerite sills and rare felsic volcanics.|
35396|Dead Bullock Formation|69288|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region. Affected by the Tanami (1835 Ma) and Stafford (1805 Ma) Events.||Tanami Group.|||Grey siltstone, silty shale, fine-grained sandstone, laminated siltstone, massive quartzite, fine-grained black shale, chert, nodular chert, amphibolite, minor calc-silicate rock.|
35396|Dead Bullock Formation|69418|6|Mentioned|p3:7|||Tanami Region. Hosts gold deposits (described).||||||12-JUL-16
35396|Dead Bullock Formation|69424|6|Mentioned|p9:4|||Tanami Region.||||Correlative of Ooradidgee Group.||12-JUL-16
35396|Dead Bullock Formation|69426|3|Fully described|p11:1, 3-7, 9, 11, 15-18, 22, 26, 30-31|Orosirian|Orosirian|Defined by Crispe et al. (2007). Incorporates the Mount Charles Beds (Blake et al., 1975), "Blake beds" and "Davidson beds" (Smith et al., 1998), MacFarlane Peak Group and Twigg Formation (Hendrickx et al., 2000). Thickness <1000m. Quiet marine conditions below storm-wave base, with increasingly deep-water deposition towards top. Hosts several major gold deposits, described in detail. The local informal mining names for constituent units are tabulated. Age from Callie Member tuff. An intrusive granite is dated at 1844 +/- 4 Ma (Smith, 2001); may reflect inherited zircons.|1838 +/- 6 Ma (Cross and Crispe, 2007).|Tanami Group.|Ferdies and Callie Members.|Is overlain conformably and transitionally by Killi Killi Formation (locally folded and sheared).|Siltstone and sandstone (Ferdies Member) fining into graphitic siltstone and banded ironstone (Callie Member); chert, schist, greywacke, mafic volcanic rocks, minor intermediate and acid volcanic rocks.|12-JUL-16
35396|Dead Bullock Formation|69587|5|Briefly described|177278.1.pdf|||Geological province: Granites-Tanami Orogen, North Australian Craton. Of Tanami Basin. ||Unit of Tanami Group.||Underlain by Killi Killi Formation.||
35396|Dead Bullock Formation|69618|4|Described|p89-96, p98-99, p100-102, p104 Fig.15|Paleoproterozoic|Paleoproterozoic|Boundary with overlying Killi Killi Formation revised upwards. See also p106, p109-110. Here includes Stubbins and Mount Charles Formations. Subdivided into Ferdies and Callie Members by Crispe and Vandenberg (2004) and Crispe et al. (2007). Also includes an informal basal unit which the authors call Kairos member. >2km thick. Cross and Crispe (2007) give a SHRIMP U-Pb zircon age of 1838 +/- 6 Ma, regarded as stratigraphically uncertain. Minimum age comes from an intrusive monzogranite SHRIMP zircon dated at 1844 +/- 4 Ma (Smith, 2001), and a lithologically similar succession from WA is dated at c.1864 Ma.|c.1864 Ma.|Unit in Tanami Group.|Includes Ferdie and Callie Members.|Is overlain by Killi Killi Formation.|Low-energy succession of chert, BIF, fine-grained pyritic and carbonaceous sedimentary rocks, and basaltic and subvolcanic dolerite sills.|30-MAR-15
35396|Dead Bullock Formation|69747|4|Described|p262-265,267,271,274|Orosirian|Orosirian|Geological province: Tanami Block, North Australian Craton. Upper stratigraphic succession represents transition zone to the overlying Killi Killi Formation. Intruded by dolerite sills (e.g. Coora, Groundrush) that have been metamorphosed to upper greenschist to amphibolite facies; deformed to the same degree as the host rock. Maximum depositional age of 1864+\-3 Ma from detrital zircons from turbiditic sandstone from top of the formation.SHRIMP and detrital ages are derived from Bagas et al, 2008.|1864+\-3 Ma (Igneous cryst. SHRIMP)|Unit of Tanami Group.|Includes former Stubbins Formation and former Mount Charles Formation, Madigan Member, Callie Member, Ferdies Member and Kairos Member.|Lower unit of the Tanami Group. Overlain conformably by Killi Killi Formation.|Mudstone, siltstone, carbonaceous siltstone, basalt (locally pillowed), common dolerite sills, and an upper succession of banded and nodular chert, greywacke and rare rhyolite.|25-JUN-19
35396|Dead Bullock Formation|69933|6|Mentioned|p11|||Similar to a weakly magnetic, unnamed unit that produced too few zircons to be dated.||||||
35396|Dead Bullock Formation|70024|6|Mentioned|p35-36|||||Tanami Group.|Callie Member.|Is overlain conformably by Killi Killi Formation.|Pelitic and psammitic schists. Underwent retrogression in the greenschist facies.|
35396|Dead Bullock Formation|70291|4|Described|p178-179,181,183,p198, 201-202|Paleoproterozoic|Paleoproterozoic|Geological province: Tanami. Restricted to eastern and central Tanami region, barely extends into WA; deposition potentially controlled by Supplejack Fault Zone along eastern depocentre margin. Shown as Dead Bullock Soak Formation on p183. Hosts the majority of the known gold resource in the tanami region.||Unit of Tanami Group.|Includes Callie Boundin Chert, Callie Member and Ferdie Member.|Basal unit of the Tanami Group. Overlain by Killi Killi Formation.|Siltstone and sandstone (Ferdie Member) fining into graphitic siltstone and BIF (Callie Member). Iron-rich sedimentary rocks occur near the stratigraphic top of the formation.|24-JUN-19
35396|Dead Bullock Formation|70478|6|Mentioned|p2 Fig 1, 12|Orosirian|Paleoproterozoic|Geological Province: Tanami. Described as undivided Dead Bullock Formation on p2 Fig 1. Minimum age from Grimwade Suite monzogranite intrusion at 1808+/-3 Ma.||Unit of Tanami Group|Includes Callie Member and Ferdies Member.|Intruded by Grimwade Suite granite.||
35396|Dead Bullock Formation|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.||Tanami Group.|Callie, Fergies Members.|Is overlain by Killi Killi Formation.||
35396|Dead Bullock Formation|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.||Tanami Group.|Ferdies, Callie Members.|Is overlain by Killi Killi Formation.||
35396|Dead Bullock Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone|
35396|Dead Bullock Formation|71349|5|Briefly described|p724-725|Paleoproterozoic|Paleoproterozoic|Tanami Region.|c.1864 Ma.|Tanami Group.||Unconformably overlies Browns Range Metamorphics. Is overlain by Killi Killi Formation.||
35396|Dead Bullock Formation|71397|5|Briefly described|p5,22,46|Orosirian|Orosirian|Geological province: Granites-Tanami Orogen.|c. 1880-1840 Ma|Unit of Tanami Group.||||
35396|Dead Bullock Formation|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1865+/-12 Ma (MDA: U-Pb zircon SHRIMP)||||Metasediment.|
35396|Dead Bullock Formation|73089|5|Briefly described|p: 1, 3-7, 10-12, 14, 17, 22-32, 41, 43|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. >1.3 km thick. Interpreted as deposited in a deep water, sediment-starved setting. Lower portion is dominantly Archean detritus. Intruded by a granitic rock with a date of 1844 +/- 4 Ma; marks minimum age constraint. 40Ar/39Ar dating of metamorphic hornblende from dolerite sills (1840 +/- 14 and 1840 +/- 19 Ma) and metamorphic monazite (1839 +/- 9 Ma) constrains an episode of metamorphism. Possibly broadly correlative to Biscay Formation.||Tanami Group|Ferdies Member, Callie Member|Transitionally overlain by Killi Killi Formation. Correlates to Mount Charles Formation and Stubbins Formation. Intruded by Inspiration Peak Monzogranite.||
35396|Dead Bullock Formation|73158|4|Described|p1, p2 Fig.1, p3, p9-11||Orosirian|Defined based on isolated outcrops and drill core. Mafic geochemical signature of volcaniclastic-sedimentary turbidite successions.|1884+/-8 Ma zircon U-Pb MDA|Tanami Group|Ferdies Member, Callie Member|Underlies Killi Killi Formation|Lower greenschist to amphibolite facies metamorphic grade. Includes tholeiitic extrusive basalts.|
35396|Dead Bullock Formation|73159|5|Briefly described|p1, p2 Fig.1, p3, 9-11|||Granites-Tanami Orogen. Defined based on isolated outcrops and drill core within the Dead Bullock Soak and The Granites goldfields. Mafic arc - backarc volcanism.|1884 +/- 8 Ma MDA: Maidment et al., 2020|Tanami Group.|Ferdies, Callie Members.|Is overlain by Killi Killi Formation.|Includes tholeiitic (extrusive) basalts. Lower greenschist- to amphibolite-facies metamorphism.|
29793|Dead Finish Tonalite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of Dougalls suite.  Age c. 1850 Ma||||||07-NOV-08
29793|Dead Finish Tonalite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tickalara Metamorphics (Lamboo Complex).  Age: 1865-1850Ma.||||||07-NOV-08
29793|Dead Finish Tonalite|43854|5|Briefly described|Map Legend||Proterozoic|||||||
29793|Dead Finish Tonalite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
29793|Dead Finish Tonalite|50437|6|Mentioned|p5.2|||Geological Province: Kimberley Region.  Of the Dougalls Suite.  See also the ?misspelt  Dead Fish Tonalite.||||||09-AUG-04
29793|Dead Finish Tonalite|66846|5|Briefly described|p558 Table 4|Orosirian|Orosirian|Age probably from U-Pb SHRIMP dating of zircon (see p547). |~1849|Of Dougalls suite.||||
29793|Dead Finish Tonalite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Tickalara Metamorphics.|||Metamorphosed hornblende-biotite(-epidote) tonalite; inclusions of metadolerite and amphibolite|
75071|Deception Hill Microgranite|63778|5|Briefly described|p1125 Fig. 1, p1126 Tb. 1, p1126, p1133|Archaean|Archaean|Age: 3023+/-10Ma (U-Pb zircon). Geological Province: Yilgarn Craton.||||||
75071|Deception Hill Microgranite|70156|4|Described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, West Australian Craton. Events: Youanmi Terrane events (3200-2600 Ma).|2786+\-26 Ma (isotopic); 2700 Ma (inferred)||||Massive, quartz- and feldspar-phyric microgranite; metamorphosed|
75071|Deception Hill Microgranite|70794|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Youanmi Terrane, Yilgarn Craton.|2787+/-26 Ma - 2700 Ma||||Massive, quartz and feldspar phyric microgranite; metamorphosed.|
75071|Deception Hill Microgranite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Youanmi Terrane.|Max age 2787+/-26 Ma, min ~2700 Ma.||||Massive, quartz- and feldspar-phyric microgranite; metamorphosed.|
79161|Decoration Sandstone|70772|4|Described|p4-9, p11, p17, p22, |Early Cretaceous||Madura Shelf. Only identified in FOR010 to date wherein it is 109m thick and is intersected between -67m and -176m and depths of 249m to 358m. Nonconformably overlies the crystalline basement. An age could not be determined from palynology and macrofossils, upper age is only constrained by dating of the overlying Loongana Formation. Deposited in a likely fluvial to intertidal or paralic environment with an aeolian source. See also p24, p28, p31, p34, p41.||||Disconformably overlain by the Loongana Formation.|Basal conglomerate, sandstone alternmating with massive fining upwards sandstone overlain by very fine-grained mudstone and claystone.|
79161|Decoration Sandstone|71618|4|Described|p122,124-130,132-133,135,137|Paleozoic|Paleozoic|Geological province: Officer Basin. Encountered in 1 well; FOR010. Thickness: 109m. Depositional environment: fluvial to intertidal/coastal with occasional aeolian influence. U-Pb ICPMS zircon analysis yield major concordant age peaks at c. 1150 and 1650 Ma, similar to the Loongana and Madura formations.  Interpreted to have experienced intense bioturbation in the basal conglomeratic section. Relative textural immaturity and differences in zircon age spectra from Officer Basin sediments suggest more proximal sediment contributions from the Albany-Fraser Orogen and Musgrave Province. minimum depositional age constrained by disconformably contact with overlying Valanginian-Hauterivian Loongana Formation.||||Overlain disconformably by Loongana Formation. Underlain unconformably by Coompana Province crystalline basement.|Red-bed sandstone; 3 main facies: 1) uppermost faintly laminated mottled green and red mudrock, 2) fining upward succession of white sandstone and thin pale green mudstone interbeds, 3) basal Fe-rich pebbly conglomerate with thick sand interbeds.|06-SEP-19
79161|Decoration Sandstone|72344|6|Mentioned|p12|Paleozoic|Paleozoic|Correlated with the red beds in CDP008.||||||
79161|Decoration Sandstone|73084|6|Mentioned|p16-18|||Officer Basin. Intersected in drillhole FOR010 below the Loongana Formation (Reynolds, 2016). Disconformably underlies Cretaceous sequence. Detrital zircon ages yield Proterozoic populations; however, the present of bioturbation indicate the unit is no older than Paleozoic.||||Disconformably overlain[?] by Loongana Formation.||
74798|Deeadeea Sandstone Member|64502|3|Fully described|p768 Fig.5||Early Permian|Of Carolyn Formation, Grant Group, Lennard shelf region. Type section location given. Thickness 19m. Overlies Ngumban Claystone Member. Poorly bedded, partly cross-bedded, mod. sorted reddish-brown sandstone with well rounded granins, probably marine.||||||27-JAN-10
74798|Deeadeea Sandstone Member|64643|4|Described|p18, 21|Sakmarian|Sakmarian|Of Carolyn Formation. Type section in Deeadeea Cliffs. Overlies Ngumban Claystone Member. Fine to medium-grained, moderately sorted sandstone ~20m thick.||||||
74798|Deeadeea Sandstone Member|65486|4|Described|p18, p22 Figs.25-26, p24 Fig.30,55|Early Permian|Early Permian|Upper unit of Carolyn Formation, Grant Group. Overlies Ngumban Claystone Member. Coarse to medium grained, crudely bedded, moderately sorted, orange to brown sandstone with well-rounded grains; probably marine. 19 m thick.||||||
74798|Deeadeea Sandstone Member|66127|3|Fully described|p213, pp283-286.|Early Permian|Early Permian|Of Playford (2002a). Named after Deeadeea Cliff. Type section from the road cut on the Great Northern Highway to the top of Deeadeea Cliff. 19 m thick.||Upper unit in Carolyn Formation.||Overlies Ngumban Claystone Member.|Poorly bedded, partly cross-bedded, moderately sorted, reddish-brown marine sandstone with well-rounded grains, possibly post-glacial aeolian; locally silicified.|
74798|Deeadeea Sandstone Member|66949|5|Briefly described|p10, p13-14, p16, p19, p57 Appx.3|Sakmarian|Sakmarian|See also p86 Appx.5. Misspelt as Deadea Sandstone Member p57. Restricted to easternmost Lennard Shelf. Outcropping type section detailed. Up to 30m thick; ?glacial non-marine deposits.||Unit in Carolyn Formation.||Overlies Ngumban Claystone Member.|Medium to coarse-grained sandstone.|02-NOV-15
23540|Defiance Dolerite|22534|6|Mentioned|Fig.5 p10|||of Kalgoorlie Group||||||
23540|Defiance Dolerite|22596|6|Mentioned|p413, Fig.5 p416|Archean|Archean|||||||07-NOV-08
23540|Defiance Dolerite|23057|4|Described|446|||||||||
23540|Defiance Dolerite|23137|4|Described|p245 Table 2|||of Kalgoorlie Group.||||||
23540|Defiance Dolerite|23139|4|Described|p234 Fig.2, p235|||||||||
23540|Defiance Dolerite|23140|5|Briefly described|p221|||||||||
23540|Defiance Dolerite|23786|5|Briefly described|p8|||Geological Province: Yilgarn Craton.||||||
23540|Defiance Dolerite|23926|6|Mentioned|p10 Tb. 1|||||||||
23540|Defiance Dolerite|24322|5|Briefly described|p61 Fig. 2|Archean|Archean|Of the Kambalda Group.||||||07-NOV-08
23540|Defiance Dolerite|24325|6|Mentioned|p61 Fig. 2|||Geological Province: Kambalda Dome, Yilgarn Craton.||||||
23540|Defiance Dolerite|41066|6|Mentioned|2 of 2 I03|||||||||
23540|Defiance Dolerite|41368|6|Mentioned|Table 1|||||||||
23540|Defiance Dolerite|41588|4|Described|p245|||||||||
23540|Defiance Dolerite|41644|6|Mentioned|p219|||||||||
23540|Defiance Dolerite|41784|6|Mentioned|Table 1|||||||||
23540|Defiance Dolerite|41890|6|Mentioned|p278|||||||||
23540|Defiance Dolerite|42117|5|Briefly described|Table 1 P67|||||||||
23540|Defiance Dolerite|42160|6|Mentioned|p45|||||||||
23540|Defiance Dolerite|42195|5|Briefly described|p154|||||||||
23540|Defiance Dolerite|42221|6|Mentioned|Table 1 P6|||||||||
23540|Defiance Dolerite|42344|5|Briefly described|p52|||||||||
23540|Defiance Dolerite|42696|6|Mentioned|Plate 1B|||||||||
23540|Defiance Dolerite|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
23540|Defiance Dolerite|42870|5|Briefly described|Table 1, P67|||||||||
23540|Defiance Dolerite|43102|5|Briefly described|Fig.3|||||||||
23540|Defiance Dolerite|43162|6|Mentioned|5|||||||||
23540|Defiance Dolerite|43496|6|Mentioned|6|||||||||
23540|Defiance Dolerite|50556|5|Briefly described|p1116 Fig.6||Archean|Eastern Goldfields Province.||||||07-NOV-08
23540|Defiance Dolerite|60514|4|Described|p27 Fig. 4, p31, p41 Fig. 11, p65 Tb. 1|Archean|Archean|Of the Paringa Basalt. Age:2680+/-8 Ma. Maximum thickness of 300m. Occurs at the base of the Paringa Basalt. Geological Province: Kambalda Domain, Yilgarn Craton.||||||02-MAY-16
23540|Defiance Dolerite|60623|4|Described|p25 Fig.2, p29|Archean|Archean|Synvolcanic base of Paringa Basalt. Conformably overlies Kapai Slate. Thickness: up to 300 m but variable. Divided into 5 zones. Geological Province: Eastern Goldfields.||||||02-MAY-16
23540|Defiance Dolerite|60627|5|Briefly described|p65 Tb.1|||Intrudes Paringa Basalt.||||||10-JUN-05
23540|Defiance Dolerite|60981|6|Mentioned|p187 Fig.6|||High - Mg Sill.||||||02-MAY-16
23540|Defiance Dolerite|62108|5|Briefly described|p1409 Tb. 15|||Of the Kalgoorlie Group. Geological Province: Yilgarn Craton (Boulder-Lefroy Shear Zone). V||||||07-FEB-11
23540|Defiance Dolerite|62111|5|Briefly described|p1459 Fig. 4|||Geological Province: Kambalda Dome in the Norseman-Wiluna greenstone belt of the Yilgarn Craton.||||||07-FEB-11
23540|Defiance Dolerite|65834|6|Mentioned|p7, 12, 44-45, 47-48|||Kambalda Domain, Kalgoorlie Terrane. Hosts the Orchin gold deposit.||Kalgoorlie Group.|||Quartz-rich.|
23540|Defiance Dolerite|67198|6|Mentioned|p116 Fig.50, p118-119, p122, p131-134|||Kambalda Sequence. The Transfer Fault may have acted as a feeder for the emplacement of this unit. Southern extent of this unit is defined by the Janus fault (which is overprinted by later intense deformation). Appears as Defiance dolerite on p133.||||||11-SEP-17
23540|Defiance Dolerite|68289|6|Mentioned|p29, p31||||c. 2690 Ma|||Intrudes the Kapai Slate and Paringa Basalt.|Laterally extensive sill of dolerite.|
23540|Defiance Dolerite|69619|6|Mentioned|p120|||St Ives area.||||Equivalent to Pernatty Dolerite.||
23540|Defiance Dolerite|69631|5|Briefly described|p25, p28|Neoarchean|Neoarchean|A laterally extensive sill; part of the greenstone succession at the Leviathan (Victory-Defiance) gold deposit.|c.2690 Ma.|||Overlies Kapai Slate; underlies Paringa Basalt.||
23540|Defiance Dolerite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2696 Ma (inferred).|Leviathan Suite|||Differentiated sill: basal pyroxenite to dolerite; granophyric phase in the central to upper sections; metamorphosed.|
23540|Defiance Dolerite|70326|5|Briefly described|p360,362-363|Neoarchean|Neoarchean|Geological province: Kambalda Domain, Kalgoorlie Terrane, Yilgarn Craton. Correlable to Turret Dolerite.|2690+\-5 Ma (Clout, 1991).|||Intrudes into upper Paringa Basalt.||
23540|Defiance Dolerite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2696 Ma (inferred)|Unit of Leviathan Suite.|||Differentiated sill: basal pyroxenite to dolerite; granophyric phase in the central to upper sections; metamorphosed|
23540|Defiance Dolerite|71308|5|Briefly described|p715|||Lesher and Arndt (1995). Of the authors' High-Th Siliceous Basalt group.|||||Basalt with distinctly layered shallow sills, with pyroxene-rich lower cumulate layers and leucogabbro upper layers.|
23540|Defiance Dolerite|72049|5|Briefly described|p258-p259|||St Ives area, occurs in the upper parts of the Kambalda Sequence.||||Intrudes the Kambalda Sequence.|Doleritic rocks.|
23540|Defiance Dolerite|72095|5|Briefly described|p10-17|||Kambalda Region, Eastern Goldfields, Yilgarn Craton. Compositionally indistinguishable from High-Th Siliceous Basalt (HTSB) of Barnes et al., 2012. Detailed geochemistry is described.||||||
23540|Defiance Dolerite|72252|6|Mentioned|p11|||St. Ives Au-Ni camp, Kambalda Domain, Yilgarn Craton. 60-100m thick.|||||Differentiated dolerite.|
23540|Defiance Dolerite|73391|5|Briefly described|Appendices.|||Cowden and Roberts (1990). Regional stratigraphic correlation chart of other workers.|||||Differentiated dolerite or flow, orthopyroxene cumulate, dolerite.|
23541|Delambre Formation|6876|6|Mentioned|p100 Fig.5.|Neogene|Neogene|||||||
23541|Delambre Formation|12491|6|Mentioned|p454 Fig.7, p457.|Holocene|Neogene|Late Miocene to Recent. Reaches maximum thickness over the edge of the Rankin/Alpha Arch trend and in the northern Exmouth Sub-basin.||||||
23541|Delambre Formation|23726|5|Briefly described|p8 Fig 2c|Quaternary|Pliocene|Underlying unit Bare Formation. Geological Province: Carnarvon Basin.||||||
23541|Delambre Formation|24084|5|Briefly described|p152 Tb.4|Pliocene|Pliocene|See also Belambre Formation (misspelt) on page 146 Fig.2. Geological Province: North Carnarvon Basin.||||||16-MAR-05
23541|Delambre Formation|40617|5|Briefly described|p17|||Mention P18||||||
23541|Delambre Formation|40800|2|Defined|p26|early Pleistocene|late Miocene|Earliest Pliocene to Late Miocene to Early Pleistocene||||||
23541|Delambre Formation|41271|3|Fully described|p189|||||||||
23541|Delambre Formation|41437|4|Described|p81|||||||||
23541|Delambre Formation|41438|6|Mentioned|p112|||||||||
23541|Delambre Formation|41732|6|Mentioned|Fig.3|||||||||
23541|Delambre Formation|42116|5|Briefly described|Fig.1 P6|||||||||
23541|Delambre Formation|43712|6|Mentioned|Fig.10,p52|Quaternary|Miocene|||||||
23541|Delambre Formation|43724|6|Mentioned|Fig.15,p65|Quaternary|Miocene|||||||
23541|Delambre Formation|61155|5|Briefly described|p5, p15|Late Pliocene|Late Miocene|Offshore, fine-grained calcareous sequence, with foraminiferal assemblages. Max. thickness (offshore): 1300m. Geological Province: Carnarvon Basin.||||||
23541|Delambre Formation|62734|5|Briefly described|p1362 Fig. 2|Holocene|Pliocene|Geological Province: Barrow Sub-basin.||||||01-SEP-08
23541|Delambre Formation|62837|5|Briefly described|Stratigraphic columns|Holocene|Late Miocene|Age: ~8-0.0Ma. Geological Province: Barrow and Dampier Sub-basins, Rankin Platform and Beagle Sub-basin.||||||01-MAR-10
23541|Delambre Formation|63950|5|Briefly described|p336 Fig. 4|Quaternary|Miocene|Geological Province: northern Carnarvon Basin.||||||27-MAY-08
23541|Delambre Formation|67200|5|Briefly described|p8 fig 6, |Quaternary|Pliocene|||||Overlies Bare Formation|Laminated siltstone beds.|
23541|Delambre Formation|67368|6|Mentioned|p209 Fig.4.|Pleistocene|Pliocene|||||||
23541|Delambre Formation|67970|6|Mentioned|p25 Fig.4.|Holocene|Messinian|Exmouth Plateau.||||||
23541|Delambre Formation|69692|6|Mentioned|p4|Quaternary|Miocene|Northern Carnarvon Basin.||||Overlies Cape Range Group.||
23541|Delambre Formation|70066|5|Briefly described|Dampier: Fig.2. Exmouth: Fig.2|Holocene|Miocene|See also Regional: Fig.6. Northern Carnarvon Basin.||||Overlies Bare Formation and Trealla Limestone.||
23541|Delambre Formation|70906|5|Briefly described|p757-758|Holocene|Pliocene|Gorgon Platform.||||Overlies Trealla Limestone (Cape Range Group).||
75843|Denham Sand|69558|5|Briefly described|p24, p66, p95, p105, p113, p234|Mid-Holocene|Pleistocene|Occupies much of the surface of Faure Island, Shark Bay. ||||Overlies the Peron Sandstone.|Red quartz and lime sands forming parabolic and transverse dunes.|
75574|Denison beds|65074|4|Described|p351, p351 fig 4-37, p353, p357 Tb. 4-12|Neoproterozoic|Neoproterozoic|Of NW Birrindudu Basin. 30m thick. Confined to Denison Range. Reference section is south of Pyramid Hill.|||||Medium-grained quartz arenite; local numerous shale pellets.|
75574|Denison beds|69440|5|Briefly described|p25:1|Cryogenian|Cryogenian|Confined to the Denison Range, SW Birrindudu Basin, in BILLILUNA map area. Lithologically similar to Lewis Range Sandstone.||||Unconformably overlies Pindar beds. Is overlain conformably by Jawilga beds. Correlates with Munyu Sandstone (NT) and (probably) Lewis Range Sandstone.|Predominantly quartz arenite.|12-JUL-16
75574|Denison beds|71080|6|Mentioned|p4|||Of Blake et al. 1977, 1979. Previously considered potential correlative of Lewis Range Sandstone. ||||||
28501|Depuch Formation|13255|6|Mentioned|p369|Middle Jurassic|Early Jurassic|Roebuck Basin.||||Overlies Bedout Formation. Is overlain unconformably by Baleine Formation.||
28501|Depuch Formation|42473|6|Mentioned|p30|||||||||
28501|Depuch Formation|43173|6|Mentioned|36|Middle Jurassic|Early Jurassic|||||||
28501|Depuch Formation|62837|5|Briefly described|Stratigraphic columns|Middle Jurassic|Early Jurassic|Age: ~203-~164Ma. Geological Province: Roebuck Basin and offshore Canning.||||||
28501|Depuch Formation|69297|5|Briefly described|p337, p339, p352|Tithonian|Hettangian|Roebuck Basin. May have some source rock potential. , ||||Overlies the Bedout Formation. Unconformably overlain by the Baleine Formation. In part equivalent to the Legendre Formation.|Coaly and algal-rich mudstones and shales.|
28501|Depuch Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Roebuck Basin.||||Overlies Bedout Formation. Is overlain by Calypso Formation.||
28501|Depuch Formation|70065|5|Briefly described|Rowley: Fig.2; p2. Regional: Fig.4; p3-5|Kimmeridgian|Hettangian|Rowley Sub-basin, Roebuck Basin and offshore Canning Basin. A thick succession of marine and marginal marine sediments including lagoonal deposits, overlain by a broad, prograding wedge of fluvio-deltaic sediments. Source rocks; fluvio-deltaic sandstones form reservoirs. Nearshore claystone beds and prodelta shales form intraformational seals.||||Overlies Bedout Formation or Murat Siltstone. Is overlain unconformably by Baleine Formation. Part-equivalent to Legendre Formation.|Includes thin coaly and algal-rich mudstones and pro-delta marine shales.|06-SEP-18
80140|Depuch Limestone|69558|5|Briefly described|p98|Pleistocene|Pleistocene|Originally the Depuch Formation of Logan et al (1970b). Renamed the Depuch Limestone in this volume. May be partly equivalent to the Bibra and Dampier Limestones. Deposited during the last interglacial period of the Pleistocene.  |||||Strongly cemented red-brown calcarenite and calcirudite.|
75770|Deserts Revenge Syenogranite|65455|6|Mentioned|p5|Neoproterozoic|Neoproterozoic|Within the Proterozoic Paterson Province. Contains clusterings of geochemical analyses with high U.||||||09-MAY-12
30349|Despair Granite|22940|5|Briefly described|p9|Paleoproterozoic|Archean|U-Pb zircon age 2.65 Ga, supersedes 'Wilthorpe granite'||||||07-NOV-08
30349|Despair Granite|23744|4|Described|p6|Archean|Archean|Age: c.2650 Ma (SHRIMP U-Pb zircon). Geological Province: Yilgarn Craton.||||||07-NOV-08
30349|Despair Granite|43830|5|Briefly described|Map Legend||Archean|Approx 2650 Ma. Narryer Terrane.||||||07-NOV-08
30349|Despair Granite|43831|5|Briefly described|Map Legend|Archean|Archean|Approx 2700 Ma||||||07-NOV-08
30349|Despair Granite|49896|6|Mentioned|p12 Fig. 8|||Massive to weakly folaited granodiorite grading into granodioritic orthogneiss. Intrudes the Psammitic schists of the Padbury Group. Within the Narryer Gneiss Terrane.||||||
30349|Despair Granite|65419|5|Briefly described|p37, p38.|Late Archean|Late Archean|Contact with Labouchere Formation is complex. Thought to be intrusive (Martin, 1994 and Windh, 1992). Slivers of the Labouchere Formation are tectonically interleaved with the Despair Granite and older gneissic granite of the Narryer Terrane, implying faulted contact.||||Is faulted against the Labouchere Formation (Padbury Group).||
30349|Despair Granite|65896|5|Briefly described|Map legend|Archean|Archean|Yilgarn Craton. Biotite granite, massive to deformed. Lenses of  biotite schist, quartzite, amphibolite, and banded iron formation.||||||
30349|Despair Granite|66112|5|Briefly described|Map legend|Paleoproterozoic|Archean|Yilgarn Craton. Biotite granite, foliated to locally massive; includes lenses of biotite schist; quartzite, banded iron-formation, and amphibolite.||||||
30349|Despair Granite|69166|5|Briefly described|geologyp_lut.csv|Neoarchean|Neoarchean||||||Biotite monzogranite, foliated to locally massive; includes lenses of biotite schist, quartzite, meta banded iron-formation, amphibolite, and quartzite|
30349|Despair Granite|70795|4|Described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Also 100k_interpgeop_lut.csv, West Australian Craton|2800-2500 Ma||||Biotite monzogranite, foliated to locally massive; includes lenses of biotite schist, quartzite, metamorphosed banded iron-formation, amphibolite, and quartzite.|
30349|Despair Granite|70796|4|Described|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean|Affected by the Capricorn Orogeny (1817  1772 Ma); Yilgarn Craton events (4000  2600 Ma). See also 500k_interpgeop14_lut.csv.|ca 2800 to 2500 Ma||||Biotite monzogranite, foliated to locally massive; includes lenses of biotite schist, quartzite, metamorphosed banded ironformation, amphibolite, and quartzite|
30349|Despair Granite|70804|5|Briefly described|p21, p43-p44, plate 1|||Hosts the Wilthorpe gold deposit.|||||Granite of alternating layers of very fine grained biotite, quartz, sericite and feldspar.|
30349|Despair Granite|70826|6|Mentioned|p9|Neoarchean|Neoarchean|Narryer Terrane.|||||Granite.|13-MAY-20
30349|Despair Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
30349|Despair Granite|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Narryer Terrane, Yilgarn Craton, West Australian Craton. Of Yarlaweelor Gneiss Complex, Capricon Orogen. Events: Capricorn Orogeny (1817-1772 Ma); Yilgarn Craton granite magmatism (3010-2600 Ma); Narryer Terrane events (4000-2600 Ma); Yilgarn Craton events (4000-2600 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv.|2800-2500 Ma (inferred)||||Biotite monzogranite, foliated to locally massive; includes lenses of biotite schist, quartzite, metamorphosed banded iron-formation, amphibolite, and quartzite|
30349|Despair Granite|71484|6|Mentioned|p125||||||||Porphyritic metagranodiorite to augen gneiss.|30-AUG-19
30349|Despair Granite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Narryer Terrane.|||||Biotite monzogranite, foliated to locally massive; includes lenses of biotite schist, quartzite, metamorphosed banded iron-formation, amphibolite, and quartzite.|
30349|Despair Granite|72259|6|Mentioned|p3|Neoarchean|Archean||ca. >2600 Ma|||||
25878|Devil Creek Formation|22694|5|Briefly described|p8|||Edmund Subgroup, Bangemall Basin||||||
25878|Devil Creek Formation|22905|5|Briefly described|p52 Fig. 2, p53 Table 1, p54|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group. Dolograinstone and dolomudstone. Conformably overlain by the Ullawarra Formation. Conformably overlies the Discovery Formation.  Max. thickness: 200m.||||||25-JAN-06
25878|Devil Creek Formation|22940|4|Described|p21|Mesoproterozoic|Mesoproterozoic|Edmund Subgroup, Bangemall Basin. Overlying unit: Nambor Sandstone. Underlying unit: Discovery Chert.||||||
25878|Devil Creek Formation|23310|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of Bangemall Group.||||||
25878|Devil Creek Formation|23311|5|Briefly described|map legend|Proterozoic|Proterozoic|Of Bangemall Group.||||||
25878|Devil Creek Formation|23403|4|Described|p7|Mesoproterozoic|Mesoproterozoic|Of Edmund Group. Consists of dolomitic breccia, dolograinstone, dolomudstone and minor stromatolites.||||||24-NOV-09
25878|Devil Creek Formation|23485|4|Described|p31|Paleoproterozoic|Paleoproterozoic|Of Edmund Group.||||||07-NOV-08
25878|Devil Creek Formation|23487|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group. Geological Province: Edmund Basin.||||||07-NOV-08
25878|Devil Creek Formation|23723|4|Described|p9 Table 1|Mesoproterozoic|Mesoproterozoic|Of Bangemall Group. Overlying unit Ullawarra Formation. U'lying unit Discovery Chert. Geological Province: Bangemall Basin. Max. thickness: 800 m.||||||
25878|Devil Creek Formation|23724|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Bangemall Group||||||
25878|Devil Creek Formation|23725|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Bangemall Group.||||||
25878|Devil Creek Formation|23780|5|Briefly described|p13|Proterozoic|Proterozoic|Of the Edmund Group.||||||
25878|Devil Creek Formation|24115|4|Described|p4 Fig.2|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group. Maximum Thickness: 200m. Overlies the Discovery Formation. Overlain by the Ullawarra Formation. Geological Province: Edmund Basin.||||||
25878|Devil Creek Formation|24183|2|Defined|p4 Fig.3, p16|Calymmian|Statherian|Of the Edmund Group (Martin et al, 1999a). Conformably overlies the Discovery Formation. Overlain gradationally by the Ullawarra Formation. Max. Thickness: 450m. Age: 1620-1462 Ma.||||||21-MAR-11
25878|Devil Creek Formation|24544|4|Described|p44 Fig.32|Mesoproterozoic|Mesoproterozoic|Of Edmund Group. Overlies Discovery Formation. Overlain by Ullawarra Formation.||||||
25878|Devil Creek Formation|29845|6|Mentioned|Table 68|||||||||
25878|Devil Creek Formation|29916|4|Described|p118|||||||||
25878|Devil Creek Formation|32720|6|Mentioned|Table 1|||||||||
25878|Devil Creek Formation|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
25878|Devil Creek Formation|34124|4|Described|Table 1|||See also p9,14. Upper Proterozoic||||||21-NOV-13
25878|Devil Creek Formation|35982|6|Mentioned|Table 22|||||||||
25878|Devil Creek Formation|36551|6|Mentioned|p101|||||||||
25878|Devil Creek Formation|36884|4|Described|p154|||||||||
25878|Devil Creek Formation|37024|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
25878|Devil Creek Formation|37213|5|Briefly described|p22|||||||||
25878|Devil Creek Formation|37460|4|Described|Table 3.VI|||||||||
25878|Devil Creek Formation|38298|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
25878|Devil Creek Formation|38299|5|Briefly described|p10|||||||||
25878|Devil Creek Formation|38988|6|Mentioned|p12|||||||||
25878|Devil Creek Formation|39210|5|Briefly described|Table 2|||||||||
25878|Devil Creek Formation|39370|5|Briefly described|p32|||||||||
25878|Devil Creek Formation|40088|6|Mentioned|p227|||||||||
25878|Devil Creek Formation|40089|2|Defined|p28|Mesoproterozoic|Mesoproterozoic|||||||
25878|Devil Creek Formation|40899|6|Mentioned|Fig.1|||||||||
25878|Devil Creek Formation|41360|6|Mentioned|p192|||||||||
25878|Devil Creek Formation|42013|5|Briefly described|Map Legend|Proterozoic||||||||
25878|Devil Creek Formation|42471|4|Described|p21|||||||||
25878|Devil Creek Formation|42472|5|Briefly described|Map legend|||||||||
25878|Devil Creek Formation|43830|5|Briefly described|Map Legend||Mesoproterozoic|||||||
25878|Devil Creek Formation|44142|4|Described|p313 Tb.4-4, p318-319, p326 Tb. 4-5|||30-800m thick. Facies changes along strike. Sub wave-base marine platform, tidal flat, estuaries, shoals of carbonate sand. Within Dooley Subgroup of Chuck (1984). Said to be a direct correlation to, and an erosion remnant of, the Bangemall Group. Is intruded by numerous dolerite sills.||Edmund Subgroup.||Overlies Discovery Chert conformably. Overlain by Nanular Sandstone and Ullawarra Formation conformably.|Dolomite (with stromatolites), shale; very minor siltstone, fine-grained sandstone, breccia, chert.|13-MAR-18
25878|Devil Creek Formation|44319|14|Not recorded|map legend||Mesoproterozoic|Bangemall Group. M.Proterozoic.||||||
25878|Devil Creek Formation|50225|4|Described|p387 Fig. 2, p394|||Of the Edmund Group (Bangemall Supergroup). Consists of dolograinstone and dolomudstone. Overlies Discovery Formation. Max. thickness: 450m. See also p390.||||||07-FEB-11
25878|Devil Creek Formation|50292|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Geological Province: Edmund Basin.  Of the Edmund Group (Bangemall Supergroup). Overlies: Discovery Formation.||||||07-NOV-08
25878|Devil Creek Formation|50312|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Edmund Group. Overlies the Discovery Formation. Geological Province: Edmund Basin. Laminated dolostone and dolomitic siltstone; local thick-bedded dolorudite.||||||31-MAY-04
25878|Devil Creek Formation|50313|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup).  Dolostone and dolomitic siltstone.  Geological Province: Edmund Basin.||||||07-NOV-08
25878|Devil Creek Formation|50380|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin.||||||07-NOV-08
25878|Devil Creek Formation|60301|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin. Dolostone and dolomitic siltstone.||||||07-NOV-08
25878|Devil Creek Formation|63470|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin. Laminated dolostone and dolomitic siltstone; local thick-bedded dolorudite.||||||24-SEP-07
25878|Devil Creek Formation|63471|5|Briefly described|Map legend|||Of the Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin. Laminated dolostone and dolomitic siltstone' locally thick-bedded dolorudite.||||||24-SEP-07
25878|Devil Creek Formation|63866|5|Briefly described|p162|||||Edmund Group||||
25878|Devil Creek Formation|63869|5|Briefly described|p28, p35-37, p53, p59-60, Plate 1|Calymmian|Statherian|85-200 m thick. Intruded by a dolerite sill aged 1465 +/- 3 Ma (Wingate, 2002). Contains manganese and chrysotile asbestos.|c.1620-1465 Ma.|Unit in Edmund Group.||Conformably overlies Discovery Formation. Is overlain gradationally by Ullawarra Formation.|Thin- to thick-bedded dolostone, dolomitic siltstone, siltstone, dolostone breccia, dolomitic sandstone, stromatolitic dolostone; minor chert.|
25878|Devil Creek Formation|64580|4|Described|map legend||Mesoproterozoic|Of Edmund Group. Siltstone and mudstone; sandstone, dolostone, dolomitic mudstone, chert, and minor conglomerate.||||||09-DEC-08
25878|Devil Creek Formation|64728|6|Mentioned|p95 Fig.2.|Mesoproterozoic|Mesoproterozoic|Deep-water siliciclastic and carbonate facies deposited below wave-base.||Unit in Edmund Group.||Overlies Discovery Formation. Is overlain by Ullawarra Formation.||
25878|Devil Creek Formation|65450|6|Mentioned|p6 Fig.4|Mesoproterozoic|Mesoproterozoic|||Edmund Group.||||05-JAN-17
25878|Devil Creek Formation|65453|5|Briefly described|map legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group. Under Ullawarra Formation; over Discovery Formation. Dolostone and dolomitic sandstone; local dolorudite. Geol. Prov: Edmund Basin.||||||
25878|Devil Creek Formation|65545|5|Briefly described|Map Legend|Mesoprotoerozoic|Paleoproterozoic|Of Edmund Group, Edmund Basin. Age: c. 1460 - <1620 Ma. Laminated dolostone and dolomitic siltstone; local thick-bedded dolorudite.||||||
25878|Devil Creek Formation|65549|5|Briefly described|Map Legend|Calymmian|Statherian|Of Edmund Group, Bangemall Supergroup, Edmund Basin. Overlies Discovery Formation; underlies Ullawarra Formation. Laminated dolostone and dolomitic siltstone; local thick bedded dolorudite||||||
25878|Devil Creek Formation|65830|4|Described|p7, p10, p16-17, p19-21; Plates 1,2|Calymmian|Statherian|85-450m thick. Prominent carbonate unit. Paleocurrent directions are mainly to the northwest and west. ||Of the Edmund Group||Conformably overlies Discovery Formation. Conformably overlain by the Ullawarra Formation.|Comprises thin- to thick-bedded dolostone, dolomitic siltstone, siltstone, dolostone breccia, dolomitic sandstone, stromatolitic dolostone, and minor chert.|
25878|Devil Creek Formation|65896|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in Edmund Group, Bangemall Supergroup. Finely bedded dolomite, dolomitic siltstone, siltstone, and minor chert.||||||
25878|Devil Creek Formation|66104|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in Edmund Group. Siltstone, dolomitic siltstone, and dolostone.||||||
25878|Devil Creek Formation|66105|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in Edmund Group. Underlies Ullawarra Formation and overlies Discovery Formation. Laminated dolostone and dolomitic siltstone; local thick-bedded dolorudite. Includes an unnamed unit of siltstone, dolomitic siltstone, and dolostone.||||||
25878|Devil Creek Formation|66110|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in Edmund Group. Metacarbonate rock; laminated dolostone and dolomitic siltstone; local thick-bedded dolorudite. Includes an unnamed unit of siltstone, dolomitic siltstone, and dolostone.||||||
25878|Devil Creek Formation|66112|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in Edmund Group. Laminated dolostone and dolomitic siltstone; local thick-bedded dolorudite.||||||
25878|Devil Creek Formation|66241|5|Briefly described|pp1-4, p6, p9. |||||Unit in Edmund Group.||Overlies Discovery Formation. Is intruded by ?Narimbunna Dolerite sills. Is overlain by Ullawarra Formation.|Deep marine-shelf planar-laminated and ripple cross-laminated dolostone, dolomitic siltstone, and sandstone.|
25878|Devil Creek Formation|66299|4|Described|pp299-303.|Mesoproterozoic|Mesoproterozoic|Metamorphosed to amphibolite facies during Edmundian Orogeny.|Inferred age between 1620 Ma and 1460 Ma.|Unit in Edmund Group.||Overlies Discovery Formation. Is overlain by Ullawarra Formation.|Metacarbonate.|
25878|Devil Creek Formation|67136|5|Briefly described|Map legend.|||Edmund Basin.||Unit in Edmund Group.||Overlies Discovery Formation. Is overlain by Ullawarra Formation.|Laminated dolostone and dolomitic siltstone; local thick-bedded dolomitic rudite.|
25878|Devil Creek Formation|67245|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Edmund Basin.||Unit in Edmund Group.||Overlies Discovery Formation. Is intruded by Narimbunna Dolerite. Is overlain by Ullawarra Formation.|Laminated dolostone and dolomitic siltstone; local thick-bedded dolorudite; siltstone.|
25878|Devil Creek Formation|67246|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Unit in Edmund Group.||Overlies Discovery Formation. Is intruded by Narimbunna Dolerite. Is overlain by Ullawarra Formation.|Laminated dolostone and dolomitic siltstone; local thick-bedded dolorudite; siltstone.|19-NOV-13
25878|Devil Creek Formation|67346|6|Mentioned|p796 Fig.3|Mesoproterozoic|Mesoproterozoic|||Of the Edmund Group.||||11-MAY-12
25878|Devil Creek Formation|67374|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Edmund Basin.||Unit in Edmund Group.|||Laminated dolostone and dolomitic siltstone; local thick-bedded dolorudite.|
25878|Devil Creek Formation|68285|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin.||Of the Edmund Group.|Informal unnamed member shown.|Underlain by the Discovery Formation. Overlain by the Ullawarra Formation.|Laminated dolostone and dolomitic siltstone; local thick-bedded dolorudite; siltstone, dolomitic siltstone, and dolostone.|
25878|Devil Creek Formation|68286|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin.||Of the Edmund Group|Informal unnamed member shown.|Underlain by the Discovery Formation. Overlain by the Ullawarra Formation.|Siltstone, laminated dolostone and dolomitic siltstone; local thick-bedded dolorudite.|
25878|Devil Creek Formation|69003|5|Briefly described|p34|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||Edmund Group.||Overlies Discovery Formation. Is overlain by Ullawarra Formation.||
25878|Devil Creek Formation|69024|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Of the Edmund Group.|||Laminated dolostone and dolomitic siltstone; local thick-bedded dolorudite.|05-MAY-14
25878|Devil Creek Formation|69027|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Of the Edmund Group.||Underlain by the Discovery Formation. Overlain by the Ullawarra Formation.|Laminated dolostone and dolomitic siltstone; local thick-bedded dolorudite.|05-MAY-14
25878|Devil Creek Formation|69028|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin. Mapped with Discovery, Ullawarra and Coodardoo Formations as one unit.||Of the Edmund Group.|||Siltstone and mudstone; sandstone, dolostone, dolomitic mudstone, chert and minor conglomerate.|06-MAY-14
25878|Devil Creek Formation|69166|4|Described|geologyp_lut.csv|Mesoproterozoic|Paleoproterozoic|||Edmund Group||Conformably overlain by Ullawarra Formation|Silicified, pyritic chert breccia, laminated dolostone and dolomitic siltstone, local thick bedded dolorudite; siltstone.|
25878|Devil Creek Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|||Part of Edmund Group, Depositiional package 4.||Unit of Edmund Group.||||
25878|Devil Creek Formation|69596|6|Mentioned|p12 Fig.7|||Edmund Basin.||Edmund Group.||||
25878|Devil Creek Formation|70019|6|Mentioned|p93-94|Mesoproterozoic|Mesoproterozoic|Geological province: Gascoyne Province, Capricorn Orogen.||Unit of Edmund Group.||Overlain by Ullawarra Formation. Underlain by Discovery Formation.||
25878|Devil Creek Formation|70127|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Edmund Group.|||Laminated dolostone and dolomitic siltstone; local thick-bedded dolorudite.|
25878|Devil Creek Formation|70132|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Edmund Basin.||Edmund Group.||Overlies Discovery Formation. Is overlain by Ullawarra Formation.|Siltstone, dolomitic siltstone, dolostone.|
25878|Devil Creek Formation|70138|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin.||Edmund Group.|||Laminated dolostone and dolomitic siltstone; local thick-bedded dolorudite.|
25878|Devil Creek Formation|70767|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin.||Edmund Group.||Overlies Discovery Formation. Is intruded by Kulkatharra Dolerite. Is overlain by Ullawarra Formation.|Laminated dolostone and dolomitic siltstone; local thick-bedded dolorudite. A sub-unit of siltstone, dolomitic siltstone, and dolostone is separately mapped.|
25878|Devil Creek Formation|70768|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin.||Edmund Group.||Overlies Discovery Formation. Is intruded by Kulkatharra Dolerite. Is overlain by Ullawarra Formation.|Laminated dolostone and dolomitic siltstone; local thick-bedded dolorudite. A sub-unit of siltstone, dolomitic siltstone, and dolostone is separately mapped.|
25878|Devil Creek Formation|70795|4|Described|100k_geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Also 100k_interpgeop_lut.csv, West Australian Craton, Edmund Basin|1590-1463 Ma|Edmund Group||Conformably overlain by Ullawarra Formation|Laminated dolostone and dolomitic siltstone; local thick bedded dolorudite, metacarbonate rock, silicified pyritic chert breccia. Siltstone, dolomitic siltstone and dolostone.|
25878|Devil Creek Formation|70814|4|Described|p3, p5, p13-p14, p20, p22, p25, p27, p49|||Edmund Basin. Together with the Discovery, Ullawarra and Coodardoo Formations forms Depositional Package 4 of the Edmund Group. This unit has a maximum thickness of 1300m. ||Edmund Group||Overlies the Discovery Formation. Conformably overlain by the Ullawarra Formation.|Stromatolitic dolomite, dolomite breccia, dolomititc siltstone, siltstone and minor diagenetic chert.|
25878|Devil Creek Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, mudstone, sandstone, dolostone, shale, dolostone/dolomite breccia, crystalline dolostone/dolomite|
25878|Devil Creek Formation|71273|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin.||Edmund Group.|||Siltstone, dolomitic siltstone and dolostone.|
25878|Devil Creek Formation|72705|5|Briefly described|p3-4|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||Edmund Group.||Overlies Discovery Formation. Is overlain by Ullawarra Formation.|Stromatolitic dolostones.|
25878|Devil Creek Formation|73442|6|Mentioned|p18|||Also referred to as part of Depositional Package 4.||||Intruded by Narimbunna Dolerite||
80958|Devonian conglomerates associated with reef complexes 80958|72034|5|Briefly described|500k_interpgeop16_lut|Famennian|Givetian|Unnamed informal unit. Lennard Shelf, Canning Basin. Age inferred.|||||Frasnian and Famennian (locally ?Givetian) boulder to cobble conglomerate and sandstone.|
26518|Dewtop Formation|30965|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
26518|Dewtop Formation|31091|6|Mentioned|p13|||||||||
26518|Dewtop Formation|33850|4|Described|Table 2|||||||||
26518|Dewtop Formation|36869|6|Mentioned|p46|||||||||
26263|Diebil Subgroup|24017|5|Briefly described|p21|||Of the Bangemall Group.||||||16-JUL-08
26263|Diebil Subgroup|40089|2|Defined|p53|Mesoproterozoic|Mesoproterozoic|||||||
26263|Diebil Subgroup|44142|6|Mentioned|p309, p310 Tb.4-3|||With eastern areas of the Collier Subgroup, has been excised (Williams, 1990) from Bangemall Group and put in the new Savory Group/Basin. Mis-spelt as Diebel Subgroup in Tb.4-3.||Savory Group||||
26263|Diebil Subgroup|50188|5|Briefly described|p10 Fig. 3, p15|||Originally of Bangemall Group, then removed to "Savory Group", now mostly Sunbeam and Disapointment Groups.||||||16-JUL-08
24244|Diemals Formation|22481|6|Mentioned|p972|||||||||
24244|Diemals Formation|22898|5|Briefly described|101|||||||||
24244|Diemals Formation|22902|4|Described|68|||Geol province Southern Cross Province||||||
24244|Diemals Formation|23526|5|Briefly described|p4 Fig. 2, p9|Archean|Archean|Clastic sedimentary rocks.  Age: <2.73Ga.||||||07-NOV-08
24244|Diemals Formation|23531|3|Fully described|p12|||SHRIMP U-Pb zircon 2729+/-9 Ma (deposition).  Also see p17 + p15. Yilgarn Craton Province.||||||
24244|Diemals Formation|23532|5|Briefly described|Map legend||Archean|Age: <c.2729 Ma. Yilgarn Craton||||||07-NOV-08
24244|Diemals Formation|23780|5|Briefly described|p87|Archean|Archean|Age: ~2729+/-9 Ma.||||||07-NOV-08
24244|Diemals Formation|23787|4|Described|p11|Archean|Archean|Age: 2729+/-9Ma (SHRIMP U-Pb).  Geological Province: Southern Cross Terrane.||||||07-NOV-08
24244|Diemals Formation|24167|3|Fully described|p25, p7 Fig.3, p34|Archean|Archean|Age: 2729+/-9Ma (SHRIMP U-Pb zircon: Nelson, 2001).||||||07-NOV-08
24244|Diemals Formation|24245|5|Briefly described|p4, p7 Tb. 1|Archean|Archean|See also p16.  Clastic sedimentary rocks.  Age: c.2730Ma (SHRIMP U-Pb zircon, Pidgeon and Wilde, 199; Nelson, 2001).  Geological Province: Yilgarn Craton.||||||07-NOV-08
24244|Diemals Formation|24335|5|Briefly described|Map legend|Archean|Archean|Age: <2733Ma.  Geological Province: Yilgarn Craton||||||07-NOV-08
24244|Diemals Formation|24445|5|Briefly described|p2 Fig.1|Archean|Archean| Geological Province: Yilgarn Craton||||||07-NOV-08
24244|Diemals Formation|24530|6|Mentioned|p2 Fig. 1|||||||||
24244|Diemals Formation|38480|2|Defined|p36|Neoarchean|Neoarchean|Also fully described p16. Age not well known but intruded by biotite adamellite with Rb/Sr whole rock age of 2.6 - 2.7 billion years. Underlying metavolcanics and graphitic phyllites are also considered to be about 2.7 billion years old.||||||09-MAY-12
24244|Diemals Formation|38483|6|Mentioned|p14|||||||||
24244|Diemals Formation|39869|6|Mentioned|Fig.5|||||||||
24244|Diemals Formation|43291|5|Briefly described|p2,Fig.2 p3.|||||||||
24244|Diemals Formation|44149|5|Briefly described|p61,p63 Tb.2-5,p67-69,p71 Fig.2-81,p76|Archean|Archean|Central part of Southern Cross Province. Clastic sedimentary rocks.||||Overlain conformably by Marda Complex.|A thick sequence of foliated conglomerate, sandstone, siltstone and argillite.  Composition of basal units is strongly dependent on underlying rocks; notably BIF clasts.|
24244|Diemals Formation|50128|5|Briefly described|p32 Fig.2, p34|Archean|Archean|Maximum depositional age: ca 2729 Ma. Geological Province: Yilgarn Craton.||||||07-NOV-08
24244|Diemals Formation|60460|4|Described|p68, 61, 63, 67, 69 fig 2-78|||||||Overlain conformably by Marda Complex. [Overlies lower greenstone belt (unconf).]|Foliated cgm, sst, siltstone and argillite.  Composition of basal units depends on underlying rocks.|
24244|Diemals Formation|61144|5|Briefly described|p13|Archean|Archean|Arenaceous and conglomerate sedimentary rocks. Geological Province: Southern Cross Province.||||||07-NOV-08
24244|Diemals Formation|63778|4|Described|p1124, p1125 Fig. 1, p1126 Tb. 1, p1126|Archaean|Archaean|Age: 2729+/-9Ma (U-Pb zircon), min age: ca. 2655Ma. Geological Province: Yilgarn Craton. Succession of siliciclastic sedimentary rocks. Detailed petrographic and chemistry information is found throughout the text.||||||18-MAR-09
24244|Diemals Formation|64771|6|Mentioned|p5|Neoarchaean|Neoarchaean|Marda-Diemals greenstone belt, Southern Cross Domain.|2730 Ma.|||||
24244|Diemals Formation|65204|6|Mentioned|p7|||West of KALGOORLIE map area. Clastic sedimentary rocks; unconformably overlies a greenstone sequence.||||||
24244|Diemals Formation|65265|5|Briefly described|p73, p74 Fig.2, p75|Neoarchean|Neoarchean|Marda-Diemals greenstone belt. Has a maximum age of c.2729 Ma; upper felsic volcanics are aged c.2720 Ma. |< c.2729 Ma; c.2720 Ma (GSWA, 2006)|Unit in Marda Complex.|||Comprises clastic sedimentary rocks; upper succession also has felsic volcanic rocks and clastic sedimentary rocks including abundant carbonaceous shales.|20-DEC-16
24244|Diemals Formation|65269|6|Mentioned|p3 Fig. 1|||Barlee 1:250 000 sheet area||||||
24244|Diemals Formation|65270|5|Briefly described|p3, p21.|Archean|Archean|Southern Cross Granite-Greenstone Terrane, Yilgarn Craton. Deposited after earliest stages of D2, the second of three deformation events in the MARMION and RICHARDSON map areas. Unconformably overlies mafic-dominated lower greenstone succession.|<c.2730 Ma (Chen et al. 2003).||||Clastic sedimentary rocks.|
24244|Diemals Formation|67198|6|Mentioned|p24|Neoarchean|Neoarchean||2729 +/- 9 Ma|||||
24244|Diemals Formation|68109|6|Mentioned|p659|Neoarchean|Neoarchean|Marda-Diemals greenstone belt, Southern Cross Domain. Chen et al. (2003).|< ca. 2729 Ma||||Clastic sedimentary.|
24244|Diemals Formation|69181|6|Mentioned|p98|||||||||
24244|Diemals Formation|69404|5|Briefly described|p7, p7 Fig.8, p8, p9|Neoarchean|Neoarchean|Southern Cross Domain, Marda-Diemals greenstone belt. Detrital zircon maximum depositional age. |c. 2701 Ma (SHRIMP U-Pb, Wingate et al., 2012)||||Conglomerate, pebbly sandstone, sandstone, siltstone, argillite and shale.|
24244|Diemals Formation|69583|5|Briefly described|p42|||Marda-Diemals greenstone belt, Southern Cross Domain.|||||Clastic sedimentary rocks.|
24244|Diemals Formation|69586|6|Mentioned|p5|||Morris et al. (2007). Youanmi Terrane.||||||
24244|Diemals Formation|70020|5|Briefly described|p117|Neoarchean|Neoarchean|Geological province: Yilgarn Craton. Clastic sequence.|c. 2730 Ma|||||
24244|Diemals Formation|70156|4|Described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma).|2701-2654 Ma (inferred)||||Sedimentary siliciclastic rocks; metamorphosed|
24244|Diemals Formation|70794|5|Briefly described|500k_interpgeop14_lut.csv,|Neoarchean|Neoarchean|Yilgarn Craton. Also 2_5m_interpgeop15_lut.csv.|2701-2654 Ma inferred.||||Sedimentary siliciclastic rocks; metamorphosed.|
24244|Diemals Formation|71168|6|Mentioned|p8, p28 fig 17, p58|||||||||
24244|Diemals Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||||||Sedimentary siliciclastic rocks; metamorphosed.|
24244|Diemals Formation|72491|5|Briefly described|p4 Fig.3, p5, 15, 19, 24, 26, 43, 45-46|||Southern Cross Terrane, Yilgarn Craton. Underwent greenschist to lower amphibolite facies metamorphism; described in detail. Paragenesis tabulated. Appears as Diemal Formation on pages 4, 5, 19, 43, 45.|||||Turbidites, metapelite schists.|
24244|Diemals Formation|73596|6|Mentioned|p1160, 1165, 1170|Neoarchean|Neoarchean|Southern Cross Domain, Youanmi Terrane. Shallow-marine to subaerial conditions. Has intraformational unconformities. Other ages given, eg 2735 +/- 7 Ma.|2729 +/- 9 Ma (MDA: Nelson, 2001).||||Polymict conglomerate, pebbly sandstone, siltstone and argillite.|
25879|Ding Dong Downs Volcanics|22496|5|Briefly described|p7|Orosirian|Orosirian|1912 +/- 3 Ma. Excluded from Halls Creek Group (referenced). Halls Creek Province.||||||09-DEC-08
25879|Ding Dong Downs Volcanics|22716|5|Briefly described|table4, p232|Orosirian|Orosirian|Age: 1910Ma||||||
25879|Ding Dong Downs Volcanics|22754|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|Of the Lamboo Complex.||||||07-NOV-08
25879|Ding Dong Downs Volcanics|23205|6|Mentioned|p42|Paleoproterozoic|Paleoproterozoic|of Halls Creek Inlier.||||||07-NOV-08
25879|Ding Dong Downs Volcanics|23323|5|Briefly described|p456 Table 1|Orosirian|Orosirian|Age: 1912 +/- 5 Ma.||||||07-FEB-07
25879|Ding Dong Downs Volcanics|23383|5|Briefly described|p12|Paleoproterozoic|Paleoproterozoic|Predominantly mafic rocks.  Age: c.1910 Ma.||||||07-NOV-08
25879|Ding Dong Downs Volcanics|23599|4|Described|p8|Paleoproterozoic|Paleoproterozoic|Age: c.1920-1910 (SHRIMP U-Pb zircon). See also page 5 Table 1. Geological Province: Lamboo Complex.||||||07-NOV-08
25879|Ding Dong Downs Volcanics|23621|3|Fully described|p14|Orosirian|Orosirian|See also page 12, table 1. Age: ~1910 Ma (isotope). Overlain by Biscay Formation. Geological Province: Halls Creek Orogen. Max. thickness >1000 m.||||||02-DEC-08
25879|Ding Dong Downs Volcanics|23622|5|Briefly described|Map Legend|Proterozoic|Archean|||||||07-NOV-08
25879|Ding Dong Downs Volcanics|24173|3|Fully described|p8, p10 Tb.1|Paleoproterozoic|Paleoproterozoic|Originally defined as part of Halls Creek Gp, now interpreted as a separate unit. Unconformably overlain by Saunders Creek Formation. Geological Province: Halls Creek Orogen. Age: c.1910Ma and 1907 +/- 6Ma. Intruded by Woodward Dolerite. See also p10 Tb.1||||||02-DEC-08
25879|Ding Dong Downs Volcanics|24572|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: >1835Ma.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
25879|Ding Dong Downs Volcanics|30892|5|Briefly described|p94|||Archaean?||||||
25879|Ding Dong Downs Volcanics|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25879|Ding Dong Downs Volcanics|32728|5|Briefly described|Table 3|||||||||
25879|Ding Dong Downs Volcanics|36551|6|Mentioned|Table 15|||||||||
25879|Ding Dong Downs Volcanics|36885|4|Described|p166|||||||||
25879|Ding Dong Downs Volcanics|37372|6|Mentioned|p17|||||||||
25879|Ding Dong Downs Volcanics|37462|4|Described|Table 4.I|||||||||
25879|Ding Dong Downs Volcanics|41976|5|Briefly described|p453|||||||||
25879|Ding Dong Downs Volcanics|41977|5|Briefly described|p471|||||||||
25879|Ding Dong Downs Volcanics|41987|6|Mentioned|Fig.3 P73|||||||||
25879|Ding Dong Downs Volcanics|42326|5|Briefly described|p9|||||||||
25879|Ding Dong Downs Volcanics|43299|5|Briefly described|Map Legend||Paleoproterozoic|of Halls Creek Group. Aged 1910+/-5 Ma.||||||07-NOV-08
25879|Ding Dong Downs Volcanics|43561|6|Mentioned|p1437|||||||||
25879|Ding Dong Downs Volcanics|43632|6|Mentioned|p9|||||||||
25879|Ding Dong Downs Volcanics|43666|6|Mentioned|p52,Table 2||Neoproterozoic|||||||
25879|Ding Dong Downs Volcanics|44155|4|Described|p234-237, p248-249|Paleoproterozoic|Paleoproterozoic|East Kimberley. Over 600m thick. Appears as Ding Ding Downs Volcanics in Tb.3-2. Basalts appear to have oceanic, rather than continental, origin.||Halls Creek Group|||Basalt, locally amygdaloidal and strongly epidotized; rhyolitic and rhyodacitic crystal tuff, crystal-lithic tuff, and tuffaceous greywacke.|
25879|Ding Dong Downs Volcanics|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Amygdaloidal metabasalt and amphibolite; metagabbro and meta-anorthosite; cordierite-bearing metamorphosed pelite. In the Lamboo Complex (eastern zone).||||||07-NOV-08
25879|Ding Dong Downs Volcanics|44317|14|Not recorded|p.5|||||||||
25879|Ding Dong Downs Volcanics|44324|14|Not recorded|p.5,16|||Tb.1. (Archaean or Proterozoic) of halls Creek Group. Contains CU mineralization.||||||
25879|Ding Dong Downs Volcanics|44325|14|Not recorded|map legend|||Archaean or Proterozoic.||||||
25879|Ding Dong Downs Volcanics|44397|14|Not recorded|p.8,9,Table 1|||Halls Creek Group. Archaean or Proterozoic.||||||
25879|Ding Dong Downs Volcanics|44398|14|Not recorded|map legend|||Archaean or Proterozoic.||||||
25879|Ding Dong Downs Volcanics|44693|5|Briefly described|Map Legend||Proterozoic|||||||
25879|Ding Dong Downs Volcanics|45047|2|Defined|p61|Proterozoic|Proterozoic|See also pp13,14.||||||02-DEC-08
25879|Ding Dong Downs Volcanics|45048|6|Mentioned|p10|||Halls Creek Group||||||
25879|Ding Dong Downs Volcanics|46797|6|Mentioned|p78|||Date given||||||
25879|Ding Dong Downs Volcanics|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Sophie Downs Suite. Age: 1912 +/- 3Ma (Shrimp).||||||07-NOV-08
25879|Ding Dong Downs Volcanics|60724|5|Briefly described|p4, p5 Fig. 2|Paleoproterozoic|Paleoproterozoic|Previously mapped within Halls Creek Group (Dow and Gemuts, 1969). Basic and felsic volcanic rocks and intercalated sedimentary rocks. Unconformably overlain by Saunders Creek Formation. Age: 1.92 - 1.90Ga. Within the Lamboo Complex.||||||07-NOV-08
25879|Ding Dong Downs Volcanics|61056|5|Briefly described|p785 Tb. 2|Paleoproterozoic|Paleoproterozoic|Age: 1912+/- 3 Ma.||||||07-NOV-08
25879|Ding Dong Downs Volcanics|61861|5|Briefly described|p9, Fig.2.|||Eastern zone of Halls Creek Orogen. Has lithological similarities with MacFarlane Peak Group.|1910 Ma (Blake et al. 1998).|||Correlated with MacFarlane Peak Group.||03-APR-12
25879|Ding Dong Downs Volcanics|63866|4|Described|p128-p130, p138|Orosirian|Orosirian|Eastern Zone, Halls Creek Orogen.|c. 1912-1907 Ma|||Overlain by the Halls Creek Group. Intruded by the Woodward Dolerite.|Bimodal volcanic rocks.|
25879|Ding Dong Downs Volcanics|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Metabasalt, amphibolite, metarhyolite, and metamorphosed sedimentry rocks, and metadolerite sills.||||||09-DEC-08
25879|Ding Dong Downs Volcanics|64662|5|Briefly described|p45, p46|Orosirian|Orosirian|SHRIMP U-Pb ages: 1907+/-6Ma, and 1912+/-3Ma (for granophyre from same unit). Is a possible source of detrital zircon in Mount Charles Formation. Rocks comprise both mafic + felsic volcanics, forming basement of eastern Halls Creek Orogen.||||||07-FEB-11
25879|Ding Dong Downs Volcanics|64722|5|Briefly described|Fig. 2 p3-6, p9|Orosirian|Orosirian|Of Halls Creek Orogen.|~1910 Ma.|||Unconformably overlain by Halls Creek Group.|Bimodal volcanic rocks.|11-APR-12
25879|Ding Dong Downs Volcanics|66526|5|Briefly described|p37.|Proterozoic|Proterozoic|Kimberley Province. Produced in the Ding Dong Downs Event, ME 5 in the Proterozoic Mafic-Ultramafic Magmatic Event Series.|c.1910 Ma.|||||
25879|Ding Dong Downs Volcanics|68078|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic||1910 Ma||||Granites and granitic volcanics.|
25879|Ding Dong Downs Volcanics|68656|5|Briefly described|GEOL_LUT_CSV/500k_geologyp08_lut|Paleoproterozoic|Paleoproterozoic||||||Metabasalt, amphibolite, metarhyolite and metamorphosed sedimentary rocks, and metadolerite sills.|
25879|Ding Dong Downs Volcanics|69003|5|Briefly described|p5, p19|Paleoproterozoic|Paleoproterozoic|E zone, Lamboo Province, Halls Creek Orogen. Coeval with Sophie Downs Suite.|c.1910 Ma.|||Is overlain by Halls Creek Group.||
25879|Ding Dong Downs Volcanics|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Data migrated from OZCHRON1. Original comment: 'This is the igneous crystallisation age of the zircon, and is thus a good stratigraphic age for the unit.'|crystallisation age: 1907+/-6 Ma U/Pb SHRIMP|Sophie Downs Suite|Includes 3 unnamed members.||Amygdaloidal metabasalt + amphibolite, metadolerite, metarhyolite, + metasedimentary rock: pelite + cordierite-bearing quartzofeldspathic rock; metarhyolite, minor metabasalt, metadolerite,+ metasedimentary rocks; metagabbro; minor meta-anorthosite|30-JUL-15
25879|Ding Dong Downs Volcanics|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv. |1907-2349 Ma|Sophie Downs Suite|Includes Sophie Downs Granophyre Member||Amygdaloidal metabasalt and amphibolite, metadolerite, metarhyolite and metasedimentary rock.|
25879|Ding Dong Downs Volcanics|69426|5|Briefly described|p11:9|Orosirian|Orosirian|Halls Creek Orogen. Mentioned as a possible source of sediment (including zircons) aged c.1910 Ma in the Mount Charles Formation.|c.1910 Ma.||||Mafic and felsic volcanic rocks.|12-JUL-16
25879|Ding Dong Downs Volcanics|69585|5|Briefly described|p2, p4|Orosirian|Orosirian|Basement to the eastern Lamboo Province.|c.1910 Ma.|||Is overlain unconformably by Halls Creek Group.|Granitic, and felsic amd mafic volcanic, rocks.|
25879|Ding Dong Downs Volcanics|69587|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Metabasalt, amphibolite, metarhyolite, and metamorphosed sedimentry rocks, and metadolerite sills|
25879|Ding Dong Downs Volcanics|69597|6|Mentioned|p5 fig 2b|||||||||
25879|Ding Dong Downs Volcanics|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|1912-1907 Ma (Isotopic)|Unit of Sophie Downs Suite.|Includes Sophie Downs Granophyre Member.||Amygdaloidal metabasalt and amphibolite, metadolerite, metagabbro; minor meta-anorthosite, metarhyolite, and metasedimentary rock; pelite and cordierite-bearing quartzofeldspathic rock.|
25879|Ding Dong Downs Volcanics|70154|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv.|1907-1912 Ma|Sophie Downs Suite|||Metagabbro; minor meta-anorthosite.|
25879|Ding Dong Downs Volcanics|70731|6|Mentioned|p268|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.||||||
25879|Ding Dong Downs Volcanics|70812|4|Described|p5-p7, p19|Orosirian|Orosirian|The oldest unit in the Eastern Zone of the Halls Creek Orogen, Lamboo Province. Misspelt as the Ding Dong Volcanics on p7.|c. 1910 Ma|Halls Creek Group||Unconformably overlain by the Halls Creek Group.|Felsic and mafic volcanic rocks.|
25879|Ding Dong Downs Volcanics|70851|4|Described|p3-p5|Paleoproterozoic|Paleoproterozoic|Eastern Zone, Lamboo Province. Misspelt as Ding Dong Volcanics on p5.|c. 1910 Ma|Sophie Downs Suite||Unconformably overlain by the Halls Creek Group.|Felsic and mafic volcanic rocks.|
25879|Ding Dong Downs Volcanics|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv and geochron files.|1912+\-3 to 1909+\6 Ma (isotopic)|Unit of Sophie Downs Suite.|Includes Sophie Downs Granophyre Member.||Amygdaloidal metabasalt and amphibolite, metadolerite, metarhyolite, and metasedimentary rock, pelite and cordierite-bearing quartzofeldspathic rock, minor meta-anorthosite|
25879|Ding Dong Downs Volcanics|71397|5|Briefly described|p1-4,8-10,19-21,27,30-33,36,42,46|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen. Crops out in the Brim Anticline, Saunders Creek Dome and Castle Creek Anticline, 20-30 km NE of Halls Creek on HALLS CREEK mapsheet. Experienced lower amphibolite facies metamorphism and are locally retrogressed to chlorite-epidote-albite-bearing assemblages. Cut by carbonate veins, alongside sheared carbonate-opaque oxides. Peperitic margins to the metabasalt units indicate contemporaneous volcanism and sedimentation, likely in a partially subaerial environment. See p19 for detailed major and trace-element geochemical analysis. Metafelsic rocks of the Ding Dong Downs Volcanics plot as rhyolite or rhyodacite. Zircon U-Pb geochronological analysis of sample GA 93526009 (foliated fragmental felsic volcanic rock) yielded a weighted mean 207Pb*/206Pb* date of 1912+\-3 Ma, interpreted as the age of volcanism. Sample GA 88598005 (fragmental felsic volcanic rock) yielded a weighted mean 207Pb*/206Pb* date of 1910+\-5 Ma, interpreted as the age of crystallisation. Sample GA GSWA 206150 (mylonitised quartzofeldspathic rock) yielded a weighted mean 207Pb*/206Pb* date of 1904+\-5 Ma, interpreted as the age of volcanic protolith.|1912-1904 Ma|Unit of Sophie Downs Suite.||||
25879|Ding Dong Downs Volcanics|71873|5|Briefly described|p427,434,442|Orosirian|Orosirian|Geological province: Lamboo Province. Emplaced during passive margin volcanism in the Eastern Zone at c. 1910-1860 Ma.|c. 1910 Ma|Unit of Sophie Downs Suite.||||
25879|Ding Dong Downs Volcanics|72437|5|Briefly described|p7, p50-53|Palaeoproterozoic|Palaeoproterozoic|Together with the Sophie Downs Granite forms basement to the Halls Creek Group.|c. 1910 Ma||||Mafic and felsic volcanic rocks, felsic schist, metabasalt, mafic schist.|
36000|Dingo Creek Granite|50225|5|Briefly described|p388|Paleoproterozoic|Paleoproterozoic|Formerly Dingo Granite of Pearson et al (1996).||||||07-FEB-11
36000|Dingo Creek Granite|50292|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Complex.  Age: 1675Ma.||||||07-NOV-08
36000|Dingo Creek Granite|61262|2|Defined|p459 App., p447 Fig. 4, p450. |Paleoproterozoic|Paleoproterozoic|Of Durlacher Supersuite. Mainly porphyritic biotite-muscovite syenogranite or syenogranite; K-feldspar phenocrysts abundant (40% plus). Intruded Pooranoo Metamorphics and Pimbyana Granite. Age: 1674+/-6Ma, 1674+/-8Ma. Type locality included.||||||07-NOV-08
36000|Dingo Creek Granite|63470|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Durlacher Supersuite. Geological Province: Gascoyne Complex. Porphyritic biotite-muscovite granite; fine- to medium-grained with thin, tabular K-feldspar phenocrysts defining a trachyte texture.||||||07-NOV-08
36000|Dingo Creek Granite|63471|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Durlacher Supersuite. Age: 1680-1620Ma. Geological Province: Gascoyne Complex. Porphyritic biotite-muscovite granite; fine- to medium-grained with thin, tabular K-feldspar phenocrysts defining a trachytic texture.||||||07-NOV-08
36000|Dingo Creek Granite|63866|4|Described|p160, p162|Statherian|Statherian|Emplaced during the Mangaroon Orogeny. Mistakenly referred to as the Dingo Granite on p162.|1674 +/- 8 Ma (SHRIMP, Nelson, 2002)|Durlacher Supersuite||Intrudes the Pooranoo Metamorphics.||
36000|Dingo Creek Granite|63869|4|Described|p19, p21-22, p24, p26, p27, Plate 1|Paleoproterozoic|Paleoproterozoic|Martin et al., (2002). Formerly the Dingo Granite of Pearson (1996); renamed to avoid confusion with the Dingo intrusion in the Pilbara. Extensive intrusion.|1674 +/- 6 Ma SHRIMP U-Pb zircon (Pearson, 1996).|Unit in Durlacher Supersuite.||Intrudes Pimbyana Granite and Pooranoo Metamorphics.|Fine- to medium-grained porphyritic biotite-muscovite monzogranite to syenogranite.|
36000|Dingo Creek Granite|65830|5|Briefly described|p30, p30 Fig.18, Plate 2|Statherian|Statherian|Formerly Dingo Granite of Pearson, 1996. This age is identical to that (1674 +/- 6 Ma) by Pearson (1996) from a sample c.30 km to the SE. Underlain by a pelitic gneiss with a detrital zircon age of around 1680 +/- 13 Ma (maximum depositional age).|1674 +/- 8 Ma (GSWA, 2006).|Unit in Durlacher Supersuite.||Intrudes Pimbyana Granite.|Fine- to medium-grained porphyritic monzogranite.|
36000|Dingo Creek Granite|66110|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Durlacher Supersuite. Porphyritic biotite-muscovite monzogranite to syenogranite; fine- to medium-grained with thin, tabular K-feldspar phenocrysts defining a trachytic texture.||||||
36000|Dingo Creek Granite|66299|4|Described|p238, pp252-253, p288.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Formerly the Dingo Granite (Pearson 1996).|1674 +/- 8 Ma.|Unit in Durlacher Supersuite.||Intensively veins a Pooranoo Metamorphics granofels unit north of James Bore. Mainly surrounded by Pimbyana Granite. Intruded by Narimbunna Dolerite sill.|Porphyritic biotite-muscovite monzogranite to syenogranite; fine- to medium-grained with thin, tabular K-feldspar phenocrysts defining a trachytic texture.|
36000|Dingo Creek Granite|68521|5|Briefly described|Map Legend|Statherian|Statherian|Geochronology from Sheppard et al. (2005).|c.1680-1620 Ma|Of the Durlacher Supersuite.|||Porphyritic biotite-muscovite monzogranite to syenogranite; fine- to medium-grained with thin, tabular K-feldspar phenocrysts defining a trachytic texture.|
36000|Dingo Creek Granite|68522|5|Briefly described|Map Legend|Statherian|Statherian|Gascoyne Province. Geochronology from Sheppard et al.(2005).|1680-1620 Ma|Of the Durlacher Supersuite.|||Porphyritic biotite-muscovite monzogranite to syenogranite; fine- to medium-grained with thin, tabular K-feldspar phenocrysts defining a trachytic texture.|
36000|Dingo Creek Granite|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Age derived from syenogranite sample (169062.1.pdf)|1674 Ma +/- 8 Ma (SHRIMP)|Durlacher Supersuite|||Porphyritic biotite--muscovite monzogranite to syenogranite; fine- to medium-grained with thin, tabular K-feldspar phenocrysts defining a trachytic texture|
36000|Dingo Creek Granite|70127|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|1682-1619 Ma.|Durlacher Supersuite.|||Porphyritic biotite-muscovite monzogranite to syenogranite, fine- to medium-grained with thin, tabular K-feldspar phenocrysts defining a trachytic texture.|09-NOV-15
36000|Dingo Creek Granite|70138|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.||Durlacher Supersuite.|||Porphyritic biotite-muscovite monzogranite to syenogranite; fine- to medium-grained with thin, tabular K-feldspar phenocrysts defining a trachytic texture.|
36000|Dingo Creek Granite|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_geologyl_lut.csv, 100k_interpgeop_lut.csv, 169062.1.pdf, 178028.1.pdf|1674 Ma||||Porphyritic biotite-muscovite monzogranite to syenogranite; fine- to medium-grained with thin, tabular K-feldspar phenocrysts defining a trachytic texture.|
36000|Dingo Creek Granite|70814|5|Briefly described|p3, p69|Statherian|Statherian||1675-1660 Ma|Durlacher Supersuite||Unconformably overlain by the Edmund Group.||
36000|Dingo Creek Granite|71869|5|Briefly described|p8, app p15|||Capricorn Orogen.|1674 +/- 8 Ma (igneous crystallisation age)|Durlacher Supersuite|||Porphyritic syenogranite, biotite muscovite syenogranite dykes.|
36000|Dingo Creek Granite|74493|6|Mentioned|p3 Fig.2|||||||||
36000|Dingo Creek Granite|74494|6|Mentioned|p1009|||||||||
31684|Dingo Intrusion|43822|5|Briefly described|map legend|Archean|Archean|Layered mafic intrusions approx. 2925 Ma. Of Pilbara Supergroup.||||||07-NOV-08
31684|Dingo Intrusion|63441|5|Briefly described|p12 Tb. 2|Archean|Archean|Of the Radley Suite. Mafic rocks.||||||07-FEB-11
31684|Dingo Intrusion|64174|5|Briefly described|Map legend|Archean|Archean|Part of the Radley Suite (Sisters Supersuite). Gabbro, leucogabbro, serpentinised peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed.||||||04-DEC-08
31684|Dingo Intrusion|64580|4|Described|map legend||Mesoarchean|Of Radley Suite. Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed.||||||15-DEC-08
31684|Dingo Intrusion|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Radley Suite.|||Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed|
31684|Dingo Intrusion|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||gabbro, anorthosite, peridotite, pyroxenite|
31684|Dingo Intrusion|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Radley Suite|||Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed.|
31790|Dinner Creek Tonalite|22547|4|Described|p12||Orosirian|Of the Paperbark supersuite.||||||14-NOV-06
31790|Dinner Creek Tonalite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.||||||07-NOV-08
31790|Dinner Creek Tonalite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1850Ma. Geological province: Kimberley Province (East).||||||07-FEB-11
31790|Dinner Creek Tonalite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
31790|Dinner Creek Tonalite|43853|5|Briefly described|Map Legend||Proterozoic|||||||
31790|Dinner Creek Tonalite|44230|5|Briefly described|Map Legend||Proterozoic|||||||
31790|Dinner Creek Tonalite|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Paperbark Supersuite.||||||07-NOV-08
31790|Dinner Creek Tonalite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Paperbark Supersuite|||Fine- to medium-grained, hypersthene-biotite-hornblende metatonalite; abundant inclusions of fine grained biotite-hornblende metatonalite|30-JUL-15
31790|Dinner Creek Tonalite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Paperbark Supersuite|||Fine- to medium-grained, hypersthene-biotite-hornblende metatonalite; abundant inclusions of fine grained biotite-hornblende metatonalite.|
31790|Dinner Creek Tonalite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone.|1864-1859 Ma (Inferred)|Unit of Paperbark Supersuite.|||Fine- to medium-grained, hypersthene-biotite-hornblende metatonalite; abundant inclusions of fine grained biotite-hornblende metatonalite|
31790|Dinner Creek Tonalite|70154|6|Mentioned|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1859-1864 Ma|Paperbark Supersuite||||
31790|Dinner Creek Tonalite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1864-1859 Ma (inferred)|Unit of Paperbark Supersuite.|||Fine- to medium-grained, hypersthene-biotite-hornblende metatonalite; abundant inclusions of fine grained biotite-hornblende metatonalite|
31790|Dinner Creek Tonalite|72437|5|Briefly described|p88-89|||Lamboo Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Biotite tonalite.|
37057|Dirk Hartog Group|1943|2|Defined|p382 p373, p375 Fig.3, p376 Fig 4|Late Silurian|Late Ordovician|Formerly Dirk Hartog Formation (Henderson and Shannon, 1966). Type section in Dirk Hartog-17B, 665-1404m.|||Comprises Hamelin Formation overlying Yaringa Evaporite overlying Ajana Formation.|Overlies Tumblagooda Group. Is overlain by Faure Formation.||
37057|Dirk Hartog Group|6943|5|Briefly described|p599-602, p604-608.|Late Silurian|Early Silurian|Carnarvon Basin. Conodont colour alteration suggests this Group has not passed oil generation window, except in Merlinleigh Sub-basin where reflectivity values imply deep burial in the Permian or effects from an intrusion. |||Includes Ajana, Yaringa and Coburn Formations.|||
37057|Dirk Hartog Group|6944|5|Briefly described|p571, p576, p577. |Silurian|Silurian|Southern Carnarvon Basin. Underlies Nannyarra Formation unconformably or disconformably. Dolomite, dolomitic limestone.||||||23-SEP-15
37057|Dirk Hartog Group|12471|6|Mentioned|p475 Fig.2. |Silurian|Silurian|||||||27-OCT-14
37057|Dirk Hartog Group|12729|4|Described|p.3-10, 20-21, 27-34|Late Silurian|Late Ordovician|Promoted to Group status (Gorter et al. 1994), superseding the 'Dirk Hartog Limestone' (Pudovskis, 1957; McWhae et al.,1958), and the 'Dirk Hartog Formation' (Playford et al., 1975).  Deposition: restricted marine environment,  brief episodes of connection to open ocean. Thickens to W.|||Ajana, Yaringa, and Coburn Formations|Conformably overlies the Tumblagooda Sandstone, unconformably underlies the Faure Formation.|Includes evaporite and carbonate rocks.|17-SEP-15
37057|Dirk Hartog Group|12731|5|Briefly described|p590, p596.|Silurian|Silurian|Thickens westward to 739 m. Organic-rich beds are more mature in northern part of Gascoyne Platform. Shows traces of gas and residual oil. Dolomite might be a potential hydrocarbon reservoir.|||Includes Coburn Formation.||Carbonates and evaporites in a restricted marine environment.|
37057|Dirk Hartog Group|12733|5|Briefly described|p554 Fig.2, pp556-564.|Silurian|Silurian|Oil and gas source in Gascoyne Platform and Merlinleigh Sub-basin. Petroleum generating potential is fair to good.||||Overlies Tumblagooda Sandstone.|Shallow marine carbonates and evaporites.|
37057|Dirk Hartog Group|13615|6|Mentioned|p73-p74|Palaeozoic|Palaeozoic|||||||
37057|Dirk Hartog Group|13996|6|Mentioned|p128|Silurian|Silurian|Subsurface Carnarvon Basin. Contains Ludlow-aged conodonts.||||||
37057|Dirk Hartog Group|14228|5|Briefly described|p4, p6 fig3, p7, p15-21|Silurian|Early Silurian|Gascoyne Platform. Maximum thickness 1100m. Thinning out to east and south. Intensely dolomitized and somewhat replaced by anhydrite cement. Seismic data do not support a hiatus below overlying Devonian rocks.|||Ajana, Yaringa and Coburn Formations.|Overlies Tumblagooda Sandstone conformably or disconformably.||05-OCT-16
37057|Dirk Hartog Group|23403|6|Mentioned|p4|||||||||
37057|Dirk Hartog Group|23572|4|Described|p3, 10|Silurian|Silurian|Geological Province: Carnarvon Basin. Underlying Unit: Tumblagooda Sandstone. Overlying Unit: Faure Formation (disconformable). Max. thickness: 740m.||||||
37057|Dirk Hartog Group|23726|5|Briefly described|p13|||Max. thickness: 739 m.||||||
37057|Dirk Hartog Group|23935|4|Described|p11 Fig.7|Pridoli|Ashgill|Conformably overlies Tumblagooda Sandstone. Unconformably overlain by Faure Formation. Interbedded light-grey to light-grey-brown dolomite and gypsum with minor shale. Geological Province: Southern Carnarvon Basin.||||||
37057|Dirk Hartog Group|24390|5|Briefly described|p19 Fig. 10|Silurian|Silurian|Geological Province: Southern Carnarvon Basin.||||||
37057|Dirk Hartog Group|49942|4|Described|p4 Fig.3, p9|Pridoli|Ashgill|Overlies Tumblagooda Sandstone. Disconformably overlain by Faure Formation. Carbonate, evaporitic and siliciclastic rocks. Geological Province: Gascoyne Platform.||||||02-MAY-13
37057|Dirk Hartog Group|50084|4|Described|p77, p77 Fig. 2, p78, p85|Silurian|Late Ordovician|Includes carbonates and evaporites deposited in subtidal, peritidal and shallow-marine evaporitic mudflat environments across the Gascoyne platform. Geological Province: Southern Carnarvon Basin.||||||02-MAY-13
37057|Dirk Hartog Group|50085|5|Briefly described|p19 Fig. 10|Silurian|Silurian|Geological Province: Southern Carnarvon Basin.||||||
37057|Dirk Hartog Group|60384|5|Briefly described|p244, p243 Fig 2a, p250, 251, p260|Late Silurian|Late Ordovician|Southern Carnarvon Basin.|||Includes Ajana, Yaringa and Coburn Formations.||Carbonate, evaporitic and siliciclastic rocks|15-NOV-12
37057|Dirk Hartog Group|60725|5|Briefly described|p28-31; p33-36 Figs.4,5,6.|Silurian|Late Ordovician|Has seal and source rocks.|||Includes Ajana, Yaringa and Coburn Formations.|Overlies Tumblagooda Sandstone.||10-MAY-17
37057|Dirk Hartog Group|61023|5|Briefly described|p34 Fig. 14|Silurian|Silurian|Geological Province: Southern Carnarvon Basin.||||||11-APR-08
37057|Dirk Hartog Group|61562|5|Briefly described|p548 Fig. 3|Silurian|Silurian|||||||
37057|Dirk Hartog Group|61563|5|Briefly described|p578 Fig. 2|Silurian|Silurian|See also p579 Fig. 3.||||||
37057|Dirk Hartog Group|61811|5|Briefly described|p7. |||Nearshore marine to marine shelf deposits.|||||Dolomite.|
37057|Dirk Hartog Group|64635|6|Mentioned|p6 |Early Silurian|Early Silurian|Thickness to 740 m.|||||Calcareous to dolomitic deposits.|
37057|Dirk Hartog Group|64972|6|Mentioned|p617 Fig. 5, p620|Silurian|Silurian|||||||
37057|Dirk Hartog Group|65313|6|Mentioned|p578, p579||Ludlovian|Contains Ludlow and Llandovery conodonts.|||Includes Ajana Formation.|Overlies Tumblagooda Sandstone.||26-MAR-12
37057|Dirk Hartog Group|65449|5|Briefly described|p34|Silurian|Silurian|Southern Carnarvon Basin. Deposited under restricted marine conditions, with brief connections to open marine environments. Correlated in part with uppermost Carribuddy Group and Worral Formation.|||Ajana, Yaringa and Coburn Formations.|Overlies Tumblagooda Sandstone.|Carbonates, evaporites and fine- to coarse-grained clastics.|
37057|Dirk Hartog Group|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||Includes Coburn Formation, Yaringa Formation, Ajana Formation.|||
37057|Dirk Hartog Group|67200|6|Mentioned|p18 table 1||||||Includes Coburn Formation, Yaringa Formation, Ajana Formation|||
37057|Dirk Hartog Group|69029|5|Briefly described|p323,326,328|Silurian|Silurian|Of onshore Carnarvon Basin. Contains good-quality and mature, but thin oil-prone source beds (Coburn-1 and Pendock-1, Gascoyne Platform).||||Overlain by Faure Formation. Underlain by Tumblagooda Sandstone.||
37057|Dirk Hartog Group|69182|6|Mentioned|Ch3 p8, Ch3 p10-p11, Ch3 p26|Silurian|Silurian|Carnarvon Basin. See also Ch3 p45, Ch3 p54-p55, Ch3 p67-p68, Ch3 p73.||||Conformably (or disconformably) overlies the Tumblagooda Sandstone.||
37057|Dirk Hartog Group|69297|6|Mentioned|p246, p249, p250|Silurian|Ordovician|Gascoyne Sub-basin of the Carnarvon Basin.|||Includes the Ajana, Coburn and Yaringa Formations.|||
37057|Dirk Hartog Group|69583|5|Briefly described|p133, p135, p139, p141, p143, Plate 4|Silurian|Silurian|Gascoyne Platform, Southern Carnarvon Basin. Contains excellent to fair, but thin, source rock intervals. Seismic interpretation. See also Dirk Hartog Formation (p131 Fig.2, p134 Fig.3, p152).|||||Carbonates.|
37057|Dirk Hartog Group|70375|6|Mentioned|p819|Silurian|Silurian|Age defined by diagnostic low-diversity conodont assemblages that range from Pridolian to the Telychian Pterospathodus celloni zone. Oldest conodonts are at least 60 m above underlying Tumblagooda Sst. ||||Overlies Tumblagooda Sandstone.||27-SEP-16
37057|Dirk Hartog Group|71146|6|Mentioned|p6, p29, p45|Silurian|Silurian|Southern Carnarvon Basin.|||Includes the Ajana Formation, Yaringa Formation and the Coburn Formation.|||
33754|Disappointment Group|22896|6|Mentioned|104|||||||||
33754|Disappointment Group|22907|2|Defined|43|Neoproterozoic III|Neoproterozoic III|Geol province Officer Basin. Age: <600 Ma. Max thickness ~1800 m. Underlying units: Sunbeam Group, Manganese Group, Boondawari Formation, Tarcunyah Group.||||||28-JUL-08
33754|Disappointment Group|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Officer Basin.||||||
33754|Disappointment Group|23590|4|Described|p14|Neoproterozoic|Neoproterozoic|Bagas et al. 1999. Geological Province: Officer Basin.||||||
33754|Disappointment Group|23730|4|Described|p12|Neoproterozoic|Neoproterozoic|Underlying unit Sunbeam Group. Geological Province: Officer Basin.||||||
33754|Disappointment Group|23758|5|Briefly described|p2 Fig 1|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
33754|Disappointment Group|23760|4|Described|p31|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
33754|Disappointment Group|24594|5|Briefly described|p602 Fig. 1|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin (Paterson Orogen).||||||
33754|Disappointment Group|49895|5|Briefly described|p12 Tb.1|Neoproterozoic|Neoproterozoic|Formerly the 'upper Savory Group'. Geological Province: Officer Basin.||||||
33754|Disappointment Group|50008|5|Briefly described|p45 Fig.2|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
33754|Disappointment Group|50188|5|Briefly described|p10 Fig. 3, p15||Neoproterozoic|Together with Sunbeam Group replaced some of the rocks of the former 'Savory Group'. Age: <600Ma. Geological Province: Earaheedy Basin.||||||16-JUL-08
33754|Disappointment Group|60470|6|Mentioned|p3, Fig. 1|Neoproterozoic|Neoproterozoic|in Officer Basin||||||
33754|Disappointment Group|61732|5|Briefly described|p56-57, p89|Ediacaran|Ediacaran|Consists of McFadden and Tchukardine Formations. Overlies Boondawari Formation; unconformably overlain by Durba Sandstone.||||||07-FEB-11
33754|Disappointment Group|62453|4|Described|p52, 59|Ediacaran|Ediacaran|Superseded upper Savory Group. Includes McFadden, Tchukardine and Woora Woora Formations. Sandstone, siltstone, conglomerate. Overlies Sunbeam Group and Boondawari Formation. Overlain by Paterson Formation. Geol. Prov: Paterson Orogen.||||||
33754|Disappointment Group|62987|5|Briefly described|p30|Neoproterozoic|Neoproterozoic|Includes the McFadden Formation. Geological Province: Officer Basin.||||||25-JAN-07
33754|Disappointment Group|63022|5|Briefly described|p1015|||Includes Lungkarta Formation. Geological Province: Officer Basin.||||||10-AUG-07
33754|Disappointment Group|64103|6|Mentioned|p400|||Geological Province: Officer Basin.||||||07-FEB-11
33754|Disappointment Group|64283|5|Briefly described|p50 Fig. 1|||Geological Province: Oldham Inlier.||||||07-FEB-11
33754|Disappointment Group|64286|5|Briefly described|p76 Fig. 4|Neoproterozoic|Neoproterozoic|Age: ~600Ma.||||||07-FEB-11
33754|Disappointment Group|64580|6|Mentioned|map legend|||||||||
33754|Disappointment Group|64722|6|Mentioned|Fig. 6 p15|Neoproterozoic|Neoproterozoic|Of Officer Basin, Centralian Superbasin.||||||
33754|Disappointment Group|64725|6|Mentioned|p67.|Neoproterozoic|Neoproterozoic|Officer Basin.||||||
33754|Disappointment Group|64772|5|Briefly described|p15, Plate 1  legend, p14 Fig. 7|Neoproterozoic|Neoproterozoic|Includes McFadden, Tchukardine and Woora Woora Formations. Age: <600Ma. Geological province: Officer Basin. See also p20-21 Fig.10||||||25-NOV-13
33754|Disappointment Group|64777|5|Briefly described|p2 Fig.3 |Neoproterozoic|Neoproterozoic|||||||
33754|Disappointment Group|65363|5|Briefly described|p18.|||||||||
33754|Disappointment Group|65454|4|Described|p6-7, p11, p30, p31|Cambrian|Neoproterozoic|Of Officer Basin. Consists of McFadden, Tchukardine and Woora Woora Formations. Disconformably overlies Sunbeam Group and Boondawari Formation. Lithological  & isotopic similarities to Supersequences 3 and 4 of Centralian Superbasin suggest 580-540 Ma age. >508 +/- 5 Ma age of intrusive dolerites.||||||21-APR-16
33754|Disappointment Group|65826|6|Mentioned|p3 Fig.1, p10. |Neoproterozoic|Neoproterozoic|Officer Basin.||||||
33754|Disappointment Group|67202|5|Briefly described|p64, p66|||NW Officer Basin.|~544 Ma.||Woora Woora, Tchukadine, McFadden Formations.|||
33754|Disappointment Group|68902|5|Briefly described|p1, p5, p25, p27|Early Cambrian|Ediacaran|Main provenance from Paterson Orogen.||||Unconformably overlies Boondawari Formation.|Includes eolian and other clastic facies.|
33754|Disappointment Group|69003|5|Briefly described|p4, p60|Neoproterozoic|Neoproterozoic|Paterson Orogen.|||Tchukardine, McFadden, Woora Woora Formations.|||
33754|Disappointment Group|69590|6|Mentioned|500k_geologyp08_lut.csv||||||Includes Tchukardine Formation, Woora Woora Formation.|||
33754|Disappointment Group|70826|6|Mentioned|p5 tbl 2|||Supersequence 4, Centralian Superbasin.||||||20-APR-20
33754|Disappointment Group|72034|6|Mentioned|500k_interpgeop16_lut|Cambrian|Ediacaran|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Durba Sandstone, Woora Woora Formation, Tchukardine Formation, McFadden Formation.|||
34912|Discovery Formation|22905|5|Briefly described|p52 Fig. 2, p53 Table 1, p54|Mesoproterozoic|Mesoproterozoic|Supersedes the Discovery Chert.  Of the Edmund Group. Overlying unit: Devil Creek Formation; underlying unit: Muntharra Formation.  Max. thickness: 500m. Contains lenticular bodies of thick-bedded, massive quartz sandstone.||||||24-JAN-06
34912|Discovery Formation|23403|4|Described|p7|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group.  Formerly Discovery Chert.  Consists of massive silicified carbonaceous mudstone and siltstone.||||||
34912|Discovery Formation|23485|4|Described|p31|Mesoproterozoic|Paleoproterozoic|Of Edmund Group.  Formerly Discovery Chert.||||||07-NOV-08
34912|Discovery Formation|23487|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group. Geological Province: Edmund Basin.||||||07-NOV-08
34912|Discovery Formation|23780|5|Briefly described|p13|Proterozoic|Proterozoic|Of the Edmund Group.||||||09-JUN-05
34912|Discovery Formation|23978|5|Briefly described|Map Legend|||Of the Edmund Group.||||||
34912|Discovery Formation|24115|4|Described|p4 Fig.2|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group. Maximum Thickness: 70m. Overlies the Muntharra Formation. Overlain by the Devil Creek Formation. Geological Province: Edmund Basin.||||||
34912|Discovery Formation|24183|2|Defined|p4 Fig.3, p14-16|Calymmian|Statherian|Of the Edmund Group (Martin et al. 1999a). Max. Thickness: 365m. Overlies the Muntharra Formation. Conformably overlain by the Devil Creek Formation. Age: 1620-1462 Ma.||||||21-MAR-11
34912|Discovery Formation|24544|5|Briefly described|p43|Mesoproterozoic|Mesoproterozoic|Of Edmund Group.||||||
34912|Discovery Formation|50188|6|Mentioned|p14|||?Of the Edmund Group.||||||16-JUL-08
34912|Discovery Formation|50225|4|Described|p387 Fig. 2, p394|||Supersedes Discovery Chert of former Bangemall Gp. Now of  Edmund Gp. An important stratigraphic marker within the Bangemall Supergroup. Cherty carbonaceous siltstone. Overlies Muntharra + Kiangi Creek Fms.  Max. thickness: 280m.||||||07-FEB-11
34912|Discovery Formation|50292|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Geological Province: Edmund Basin.  Of the Edmund Group (Bangemall Supergroup). Underlies: Devil Creek Formation.||||||07-NOV-08
34912|Discovery Formation|50312|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Edmund Group. Overlies the Kiangi Creek Formation. Overlain by Devil Creek Formation. Geological Province: Edmund Basin. Massive or laminated chert, mudstone and siltstone.||||||31-MAY-04
34912|Discovery Formation|50313|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup).  Geological Province: Edmund Basin. Overlies Kiangi Creek Formation.||||||07-NOV-08
34912|Discovery Formation|50380|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin.||||||07-NOV-08
34912|Discovery Formation|60301|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin. Chert, carbonaceous siltstone and mudstone.||||||07-NOV-08
34912|Discovery Formation|63470|5|Briefly described|Map legend|Mesoproterozoic||Of the Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin. Massive or laminated chert, silicified mudstone, siltstone; local silicified sandstone and conglomerate.||||||24-SEP-07
34912|Discovery Formation|63471|5|Briefly described|Map legend|||Of the Edmund Group (Bangemall Supergroup). Overlain by Devil Creek Formation; overlies Kiangi Creek Formation. Geological Province: Edmund Basin. Massive and laminated chert, silicified mudstone, and siltstone.||||||24-SEP-07
34912|Discovery Formation|63866|5|Briefly described|p162|||||Edmund Group||||
34912|Discovery Formation|63869|4|Described|p28, p34-35, p45, p46, p59, Plate 1|Calymmian|Statherian|Formerly Discovery Chert; renamed because chert was not the dominant lithology. A major regional marker horizon. 50-365 m thick. Intruded by a dolerite sill aged 1465 +/- 3 Ma (Wingate, 2002). Hosts stratabound Cu and Zn mineralisation at Mount Palgrave and S of Illirie Bore.|c.1620-1465 Ma.|Unit in Edmund Group.||Disconformably overlies Muntharra Formation or Kiangi Creek Formation. Is overlain by Devil Creek Formation.|Planar-laminated, pyritic, silicified carbonaceous siltstone, with cubic and rhombohedral mineral casts after pyrite or evaporites; local beds of silicified sandstone, pebble conglomerate and sedimentary breccia occur.|
34912|Discovery Formation|64283|5|Briefly described|p53|||Of the Edmund Group (Bangemall Supergroup).||||||07-FEB-11
34912|Discovery Formation|64287|5|Briefly described|p31, p34 Fig. 2|||Superseded Discovery Chert. Laminated chert unit on EDMUND sheet.||||||07-FEB-11
34912|Discovery Formation|64580|4|Described|map legend||Mesoproterozoic|Of Edmund Group. Siltstone and mudstone; sandstone, dolostone, dolomitic mudstone, chert, and minor conglomerate.||||||15-DEC-08
34912|Discovery Formation|64728|6|Mentioned|p95 Fig.2, p104.|Mesoproterozoic|Mesoproterozoic|Deep-water siliciclastic and carbonate facies deposited below wave-base.||Unit in Edmund Group.||Overlies Muntharra Formation. Is overlain by Devil Creek Formation.||
34912|Discovery Formation|65450|6|Mentioned|p5 Fig.2, p6 Fig.4|Mesoproterozoic|Mesoproterozoic|||Edmund Group||||
34912|Discovery Formation|65453|5|Briefly described|map legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group. Over Kiangi Creek Formation; under Devil Creek Formation. Chert, silicified mudstone and siltstone; local silicified sandstone and conglomerate. Geol. Prov: Edmund Basin.||||||
34912|Discovery Formation|65545|5|Briefly described|Map Legend|Mesoprotoerozoic|Paleoproterozoic|Of Edmund Group, Edmund Basin. Age: c. 1460 - <1620 Ma. Massive or laminated chert, silicified mudstone, and siltstone; local silicified sandstone and conglomerate.||||||
34912|Discovery Formation|65549|5|Briefly described|Map Legend|Calymmian|Statherian|Of Edmund Group, Bangemall Supergroup, Edmund Basin. Overlies Kiangi Creek Formation; underlies Devil Creek Formation. Massive or laminated chert, silicified mudstone, and siltstone; local silicified sandstone and conglomerate.||||||
34912|Discovery Formation|65830|4|Described|p4, p6, p7, p10, p12, p16, p19-21|Calymmian|Statherian|See also Plates 1-2. Recognised as a major regional marker. 50-365 m thick. Deep-marine-shelf deposit. Higher energy deposits are locally abundant. Contains large chert olistoliths.||Of the Edmund Group||Underlain disconformably by the Muntharra Formation or Kiangi Creek Formation. Conformably overlain by the Devil Creek Formation or Ullawarra Formation.|Basal silicified sandstone and conglomerate. Planar-laminated, pyritic, silicified carbonaceous siltstone ("chert") with mineral casts. Comprises a lower unit characterised by pinch-and-swell structures and an upper planar laminated unit.|
34912|Discovery Formation|65896|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in Edmund Group, Bangemall Supergroup. Planar parallel-laminated to locally wavy beds of cream to black chert and siltstone.||||||
34912|Discovery Formation|66104|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in Edmund Group. Massive or laminated chert, silicified mudstone, and siltstone; local silicified sandstone and conglomerate. Includes a mapped but unnamed unit of siltstone.||||||
34912|Discovery Formation|66105|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in Edmund Group. Overlies Kiangi Creek Formation and underlies Devil Creek Formation. Massive or laminated chert, silicified mudstone and siltstone; local silicified sandstone and conglomerate. ||||||
34912|Discovery Formation|66110|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in Edmund Group. Massive or laminated chert, silicified mudstone, and siltstone; local silicified sandstone and conglomerate; metamorphosed silicified mudstone, locally with abundant pyrite.||||||
34912|Discovery Formation|66112|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in Edmund Group. Massive or laminated chert; silicified mudstone, and siltstone; local silicified sandstone and conglomerate.||||||
34912|Discovery Formation|66241|5|Briefly described|pp1-4, p6, p9. |||||Unit in Edmund Group.||Disconformably overlies Muntharra and Kiangi Creek Formations. Is intruded by ?Narimbunna Dolerite sills. Is overlain by Devil Creek Formation.|Chert and silicified siltstone.|
34912|Discovery Formation|66299|4|Described|pp299-303.|Mesoproterozoic|Mesoproterozoic|A series of thin, discontinuous, poorly exposed outcrops. Individual beds are about 10-15 cm thick, defined principally by colour variations. Interpreted as an overstep on Kiangi Creek Formation.|Inferred age between 1620 Ma and 1460 Ma.|Unit in Edmund Group.||Oversteps Kiangi Creek Formation. Conformably overlain by Devil Creek Formation, with Narimbunna Dolerite locally intruded between them.|Metamorphosed silicified mudstone, light blue-grey, very fine-grained; conchoidal and feathery fracture; locally with abundant pyrite.|
34912|Discovery Formation|67136|5|Briefly described|Map legend.|||Edmund Basin.||Unit in Edmund Group.||Overlies Kiangi Creek Formation. Is overlain by Devil Creek Formation.|Massive or laminated chert, silicified mudstone, and siltstone; local silicified sandstone and conglomerate.|
34912|Discovery Formation|67245|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Edmund Basin.||Unit in Edmund Group.||Overlies Kiangi Creek Formation. Overlies and is intruded by Narimbunna Dolerite. Is overlain by Devil Creek Formation.|Massive or laminated chert, silicified mudstone, and siltstone; local silicified sandstone and conglomerate.|
34912|Discovery Formation|67246|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Unit in Edmund Group.||Overlies Kiangi Creek Formation. Is intruded by Narimbunna Dolerite. Is overlain by Devil Creek Formation.|Massive or laminated chert, silicified mudstone, and siltstone; local silicified sandstone and conglomerate.|19-NOV-13
34912|Discovery Formation|67346|6|Mentioned|p795 Fig.2, p796 Fig.3|Mesoproterozoic|Mesoproterozoic|||Of the Edmund Group.||||11-MAY-12
34912|Discovery Formation|67374|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Edmund Basin.||Unit in Edmund Group.|||Massive or laminated chert, silicified mudstone, and siltstone; local silicified sandstone and conglomerate.|
34912|Discovery Formation|68285|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin.||Of the Edmund Group.|Informal unnamed siltstone member shown.|Underlain by the Kiangi Creek Formation. Overlain by the Devil Creek Formation.|Massive or laminated chert, silicified mudstone, and siltstone; local silicified sandstone and conglomerate; siltstone.|
34912|Discovery Formation|68286|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin.||Of the Edmund Group|Informal unnamed siltstone member shown.|Underlain by the Kiangi Creek Formation. Overlain by the Devil Creek Formation.|Massive or laminated chert, silicified mudstone, and siltstone; local silicified sandstone and conglomerate.|
34912|Discovery Formation|69003|5|Briefly described|p34|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||Edmund Group.||Overlies Muntharra Formation. Is overlain by Devil Creek Formation.||
34912|Discovery Formation|69024|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Of the Edmund Group.|||Massive or laminated chert, silicified mudstone, and siltstone; local silicified sandstone and conglomerate.|05-MAY-14
34912|Discovery Formation|69027|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Of the Edmund Group.||Overlies Muntharra Formation. Overlain by the Devil Creek Formation.|Massive or laminated chert, and silicified mudstone, and siltstone; local silicified sandstone and conglomerate.|05-MAY-14
34912|Discovery Formation|69028|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin. Mapped with Devil Creek, Ullawarra and Coodardoo Formations as one unit.||Of the Edmund Group.|||Siltstone and mudstone; sandstone, dolostone, dolomitic mudstone, chert and minor conglomerate.|06-MAY-14
34912|Discovery Formation|69166|4|Described|geologyp_lut.csv|Mesoproterozoic|Paleoproterozoic|||Edmund Group||Overlies Kiangi Creek Formation|Massive or laminated chert, silicified metamudstone and mudstone, siltstone; local silicified sandstone and conglomerate.|
34912|Discovery Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|||Part of Edmund Group, Depositiional package 4.||Unit of Edmund Group.||||
34912|Discovery Formation|69596|6|Mentioned|p12 Fig.7, p17|||Edmund Basin.||Edmund Group.||||
34912|Discovery Formation|70019|6|Mentioned|p93-94|Mesoproterozoic|Mesoproterozoic|Geological province: Gascoyne Province, Capricorn Orogen.||Unit of Edmund Group.||Overlain by Devil Creek Formation. Underlain by Muntharra Formation.||
34912|Discovery Formation|70127|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Edmund Group.|||Metamorphosed silicified mudstone; locally with abundant pyrite.|
34912|Discovery Formation|70132|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Edmund Basin.||Edmund Group.||Overlies Kiangi Creek Formation. Is overlain by Devil Creek Formation.|Massive or laminated chert, silicified mudstone, and siltstone; local silicified sandstone and conglomerate.|
34912|Discovery Formation|70138|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin.||Edmund Group.||Overlies Kiangi Creek Formation. Is intruded by Narimbunna Dolerite.|Massive or laminated chert, silicified mudstone, and siltstone; local silicified sandstone and conglomerate.|
34912|Discovery Formation|70767|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin.||Edmund Group.||Overlies Kiangi Creek Formation. Is overlain by Devil Creek Formation.|Massive or laminated chert, silicified mudstone, and siltstone; local silicified sandstone and conglomerate.|
34912|Discovery Formation|70768|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin.||Edmund Group.||Overlies Kiangi Creek Formation. Is overlain by Devil Creek Formation.|Massive or laminated chert, silicified mudstone, and siltstone; local silicified sandstone and conglomerate.|
34912|Discovery Formation|70795|4|Described|100k_geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Also 100k_geologyl_lut.csv, 100k_interpgeop_lut.csv, 156614.1.pdf, 189223.1.pdf, West Australian Craton, Edmund Basin|1590-1465 Ma|Edmund Group||Overlies Kiangi Creek Formation|Massive or laminated chert, silicified mudstone, siltstone; local silicified sandstone and conglomerate. Metamorphosed silicified mudstone; locally with abundant pyrite.|
34912|Discovery Formation|70814|4|Described|p3, p5, p12-p14|||Edmund Basin. Together with the Devil Creek, Ullawarra and Coodardoo Formations forms Depositional Package 4 of the Edmund Group. This unit is thickest in the southwestern, southern and southeastern parts of the Edmund Basin where it ranges from 280 to 300m thick. Lithology discussed in detail. This unit is interpreted to have been deposited in a starved anoxic environment below storm-wave base. This formation was believed to have been deposited between c. 1590 and 1465 Ma based on ages of overlying and underlying stratigraphic units. See also p20, p22, p25, p27, p33, p49.||Edmund Group||Overlies the Muntharra Formation. Overlain by the Devil Creek Formation.|Massive or laminated chert, together with silicified mudstone and siltstone and minor silicified sandstone and conglomerate.|
34912|Discovery Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, mudstone, sandstone, dolostone, chert|
34912|Discovery Formation|71273|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin.||Edmund Group.|||Massive or laminated chert, silicified mudstone, and siltstone; local silicified sandstone and conglomerate.|
34912|Discovery Formation|72705|5|Briefly described|p3-4|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||Edmund Group.||Unconformably overlies Muntharra Formation. Is overlain by Devil Creek Formation.|Carbonaceous siltstone and chert.|
34912|Discovery Formation|73442|6|Mentioned|p18|||Also referred to as part of Depositional Package 4.||||Intruded by Narimbunna Dolerite||
30803|Discretion Granite|22940|6|Mentioned|p13|||||||||
30803|Discretion Granite|23485|5|Briefly described|p30|Statherian|Statherian|Age: 1619+/-15Ma.||||||
30803|Discretion Granite|23592|5|Briefly described|p9 Table 1|Paleoproterozoic|Paleoproterozoic|Age: 1619+/-15 Ma.||||||07-NOV-08
30803|Discretion Granite|23780|5|Briefly described|p21|Statherian|Statherian|Age: ~1644+/-6 Ma||||||
30803|Discretion Granite|24544|5|Briefly described|p11 Fig.7|Statherian|Statherian|Age: 1600-1640 Ma.||||||
30803|Discretion Granite|43830|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
30803|Discretion Granite|50216|5|Briefly described|p213|Paleoproterozoic|Paleoproterozoic|Of the northern Gascoyne Complex. Age: 1619+/-15 Ma (Sheppard and Swager, 1999).||||||07-NOV-08
30803|Discretion Granite|50221|5|Briefly described|p312|Paleoproterozoic||Age: 1619+/-15 Ma.||||||07-NOV-08
30803|Discretion Granite|50225|5|Briefly described|p397|||Of the Gascoyne Complex.  Age: 1619+/-15Ma (Nelson, 1998; Sheppard and Swager, 1999).  In faulted contact with the Bangemall Supergroup.||||||07-FEB-11
30803|Discretion Granite|61262|5|Briefly described|p458 App.|Paleoproterozoic|Paleoproterozoic|Massive porphyritic biotite monzogranite. Intrudes the Yarlarweelor Gneiss Complex. Age: ca.1620Ma.||||||07-NOV-08
30803|Discretion Granite|63866|5|Briefly described|p162|Statherian|Statherian|This is the youngest granite in the Gascoyne Complex.|1619 +/- 15 Ma (Nelson, 1998)|||||
30803|Discretion Granite|63869|5|Briefly described|p29|Statherian|Statherian|The youngest granite in the Gascoyne Complex. [geochron report 142855.1.pdf, Nelson (1998)].|1619 +/- 15 Ma (GSWA, 2005).|Unit in Gascoyne Complex.||||09-MAR-18
30803|Discretion Granite|65549|5|Briefly described|Map Legend|Statherian|Statherian|Of Durlacher Supersuite. Medium grained, porphyritic biotite monzogranite; tabular phenocrysts of K-feldspar. Age of c. 1620 Ma given for Supersuite.||||||
30803|Discretion Granite|65896|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|c.1619 Ma. Medium-grained, porphyritic, biotite monzogranite; tabular phenocrysts of K-feldspar. Unnamed sub-unit dated at c. 1645 Ma||||||
30803|Discretion Granite|66112|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Aged c.1620 Ma. Shown as only constituent of Durlacher Supersuite. Medium-grained, porphyritic biotite monzogranite; tabular phenocrysts of K-feldspar.||||||
30803|Discretion Granite|66299|4|Described|p45, p247-248, p254-257.|Paleoproterozoic|Paleoproterozoic|Narryer Terrane, Yilgarn Craton.|1644 +/- 6 Ma to main phase 1619 +/- 15 Ma.|||Intrudes Yarlarweelor Gneiss Complex and Moorarie Supersuite.|Medium- to coarse-grained, porphyritic monzogranite with tabular K-feldspar phenocrysts.|17-AUG-22
30803|Discretion Granite|66950|5|Briefly described|p12|Statherian|Statherian||c. 1620 Ma|Of the Durlacher Supersuite.||||
30803|Discretion Granite|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Age derived from xenolith sample (168751.1.pdf)|1644 Ma +/- 6 Ma (SHRIMP) |Durlacher Supersuite|||Fine- to medium-grained, porphyritic biotite monzogranite; tabular phenocrysts of K-feldspar. Medium grained porphyritic biotite monzogranite.|
30803|Discretion Granite|69596|5|Briefly described|p13|||Northern margin of the Yilgarn Craton. Associated with the 1680-1620 Ma Mangaroon Orogeny.|c.1620 Ma.|Durlacher Supersuite.||||
30803|Discretion Granite|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|100k_interpgeop_lut.csv, 168751.1.pdf|1644-1619 Ma||||Equigranular or medium grained, porphyritic biotite monzogranite, tabular phenocrysts of K feldspar. Fine to medium grained porphyritic biotite monzogranite, tabular phenocrysts of K-feldspar.|
30803|Discretion Granite|70814|5|Briefly described|p3, p67|Statherian|Statherian||1644-1619 Ma|Durlacher Supersuite||Faulted against the Edmund Group.||
30803|Discretion Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
30803|Discretion Granite|71869|5|Briefly described|p3-p4, p8, p10-p12, p15-p18, app p17|||Gascoyne Province. Emplaced during the Mangaroon Orogeny. Oxygen analyses are discussed.||Durlacher Supersuite||||
77448|Ditji Formation|67354|3|Fully described|p75, pp93-97, p103, p106.|Sakmarian|Sakmarian|New name. Named after Ditji Beach. Type section is between 1,721 m and 1,795 m in Kinmore-1; a reference section is 1,079 m to 1,132 m in Barnett-1. Bonaparte Basin. Probably deposited in a marginal marine environment; apparently correlative with Fossil Cliff Sandstone (Perth Basin), Callytharra Formation (Carnarvon Basin) and Nura Nura Member of the Poole Sandstone (Canning Basin). Has reservoir potential.|c.291 Ma.|||Overlies, probably unconformably, the Quoin Formation.|Hard calcareous sandstone grading to sandy limestones (sparite cement in coarse-grained sandstone); minor coal interbeds; a distinctive bed with high radioactivity and density, low resistivity and sonic velocity: possibly bentonite from volcanic ash.|
77448|Ditji Formation|69452|4|Described|p36:8, 15, 18-19|Sakmarian|Sakmarian|Gorter et al. (2008). Originally included in the Keyling Formation (Mory, 1991). Petrel Sub-basin, Bonaparte Basin. Marine or marginal marine deposits. Up to 130m thick. Offshore.||Kulshill Group.||Overlies Quoin Formation, probably unconformably. Is overlain by Keyling Formation, probably unconformably.|Calcareous sandstone grading to sandy limestone with minor interbeds of coal.|12-JUL-16
77448|Ditji Formation|69454|5|Briefly described|p38:4|Sakmarian|Sakmarian|Petrel Sub-basin, Bonaparte Basin.||Kulshill Group.||||12-JUL-16
77448|Ditji Formation|69653|6|Mentioned|p10|Cisuralian|Cisuralian|Petrel Sub-basin.||Kulshill Group.||Overlies Quoin Formation. Is overlain by Keyling Formation.||
77448|Ditji Formation|69673|5|Briefly described|p153 fig 125, p168 fig 141, p173|Permian|Carboniferous|||Kulshill Group||Overlain by Keyling Formation, overlies Quoin Formation|Calcareous sandstone grading to sandy limestone with minor coal interbeds.|
77448|Ditji Formation|70061|5|Briefly described|Petrel Sub-basin Figs.2 & 3|Sakmarian|Sakmarian|See also Regional geology: Fig.8.||Kulshill Group.||Overlies Quoin Formation. Is overlain by Keyling Formation.||12-JUL-16
77448|Ditji Formation|72505|5|Briefly described|p889-p890|Sakmarian|Sakmarian|Southern Bonaparte Basin. Correlated with the P. Confluens zone and the Pseudoreticulaspora pseudoreticulata zones. Includes a tuff bed.||||Overlies the Quoin Formation. Overlain by the Keyling Formation.||12-MAR-20
77448|Ditji Formation|73117|6|Mentioned|p14-15|Asselian|Asselian|Bonaparte Basin. Age is from a volcanic ash bed (see Gorter et al., 2005).|c. 295 Ma|Kulshill Group||Underlain by Quoin Formation. Overlain by Keyling Formation.||
33872|Dixie Sill|22534|5|Briefly described|p21|||||||||
73622|Dixon Island Formation|24391|4|Described|p8-4 Fig.2|Archean|Archean|Of Cleaverville Group. Felsic volcanics, black-white chert, felsic tuff, ferruginous chert and banded iron formation. Overlies Lagoon Pillow Basalt. Overlain by Dixon Pillow Basalt. Geological Province: Pilbara Block.||||||07-NOV-08
73622|Dixon Island Formation|63518|5|Briefly described|p753|Archean|Archean|A north eastern extension of the Cleaverville greenstone belt, interpreted as oceanic sea-floor of an immature island arc, based on basaltic and rhyolitic bimodal volcanism.||||||07-NOV-08
73622|Dixon Island Formation|66118|5|Briefly described|p147|||Pilbara Craton. West Pilbara Superterrane. Age: U-Pb zircon date from 20cm thick layer of felsic tuff within bedded black siliceous shales, Kiyokawa et al. 2002.|3195+/-15 Ma SHRIMP U-Pb zircon felsic tuff|||||
73622|Dixon Island Formation|66882|5|Briefly described|p118|Mesoarchean|Paleoarchean|West Pilbara Craton. A possible source for Mesoarchean zircons in Cook Gap Schist (Gawler Craton).|3195+/-15 Ma (Kiyokawa et al., 2002).||||Volcanics.|
73622|Dixon Island Formation|67201|4|Described|p12 Tb.1, p14|Archean|Archean|Recognised only on Dixon Island. In northwestern Pilbara Craton, West Pilbara Superterrane, Regal Terrane. In informal Cleaverville succession with Port Robinson Basalt and Regal Formation.|3195 Ma, U-Pb zircon, felsic tuff|||Is overlain by Regal Formation (on Dixon Island).|Includes thin felsic tuff.|22-NOV-16
73622|Dixon Island Formation|67721|6|Mentioned|p37|Mesoarchean|Paleoarchean|Contains c. 3200 Ma volcanic rocks.||||||
73622|Dixon Island Formation|68574|4|Described|p1, p3-7, p9, p12-14|Mesoarchean|Mesoarchean|Kiyokawa and Taira (1998), for a previously unnamed part of the Cleaverville Formation. Formalised in this Record. NW Pilbara Craton. 400m thick. Reported to contain a hydrothermal vent system with possible microbial material. Drillcore logs and drillcore tray photographs. SHRIMP U-Pb zircon age from a thin felsic tuff unit.|3195 +/- 15 Ma (Kiyokawa et al., 2002).|||Interpreted to overlie Regal Formation. Is overlain by Port Robinson Basalt.|Extremely silicified, basal tuffaceous rocks, overlain by black chert (containing up to 2% by weight organic carbon), above which is a multi-coloured chert and shale unit.|
73622|Dixon Island Formation|69301|5|Briefly described|p9 Tb.1, p13, p20 Tb.2, p22|||Pilbara Craton. West Pilbara Superterrane. Regal Terrane. Crops out only along the northwest Pilbara coast near Cleaverville, where it underlies pillow basalts here assigned to the Regal Formation. Age: zircon from a thin felsic tuff unit (Kiyokawa et al. 2002).|3.19 Ga U-Pb zircon, see comments|||Underlies Regal Formation on northwest Pilbara coast near Cleaverville.||
73622|Dixon Island Formation|70775|4|Described|p12, p19, p26, p28-p29, p48|Mesoarchean|Paleoarchean|Nickol River Basin. Also dated at c. 3195 +/- 15 Ma by Kiyokawa et al., 2002.|3220-3160 Ma|||Overlies the Roebourne Group (Weerianna Basalt). Overlain by the Regal Formation. Overlain by (or is sheared against) the Port Robinson Basalt. Equivalent to the Nickol River Formation.|Black carbonaceous shale, chert and minor felsic volcanic rocks.|
73622|Dixon Island Formation|71349|6|Mentioned|p738|||Extensive sedimentary sequence. Resulted from c.3.2 Ga rifting of the Pilbara.||||||
81737|Dixon Range Formation|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|1030-1030 Ma (inferred)|Unit of Tjauwata Group.|||Quartz- to quartzofeldpathic sandstone interbedded with siltstone; ferruginous sandstone and siltstone, fine-grained conglomerate, polymict conglomerate, stromatolitic dolostone, heavy mineral bands.|
23546|Djigumirri Member|13194|6|Mentioned|p395 Tb. 4-16, p399 fig 4-63|||Type Section: Hart Spring 15o19'S 128o27'E. 7.5-22m thick protected subtidal system.||Skewthorpe Formation||Overlies Galawa Member (conformably). Overlain by Bolgumirri Member (conformably).|Siltstone, sandstone and sandy dolomite.|
23546|Djigumirri Member|40993|6|Mentioned|Fig.1|||||||||
23546|Djigumirri Member|41864|4|Described|p38|||||||||
23547|Djilirri Limestone|13194|4|Described|p392 Tb. 4-16, p402 fig 4-66|Early Famennian|Early Famennian|Type Section: Surprise Creek 15o11'S 128o37'E||Ningbing Group||Overlies Hargreaves Formation (conformably). Laterally equivalent to Kamilili Formation.|Peloidal limestone, algal boundstone, and limestone breccia.|
23547|Djilirri Limestone|40993|2|Defined|p7|Famennian|Famennian|||||||
23547|Djilirri Limestone|41864|3|Fully described|p86|||Formerly "Ningbing Limestone" and Jeremiah Member"||||||
23547|Djilirri Limestone|41865|5|Briefly described|Map legend|middle Famennian|early Famennian|||||||
23547|Djilirri Limestone|41867|5|Briefly described|Map legend|middle Famennian|early Famennian|||||||
23547|Djilirri Limestone|42933|5|Briefly described|Fig.94 p258|||||||||
23547|Djilirri Limestone|69452|6|Mentioned|p36:7|||||Ningbing Group.||||12-JUL-16
23547|Djilirri Limestone|69673|6|Mentioned|p169|||||Ningbing Group||Overlain by Kamilili Formation||
74634|Djugun Member|64449|2|Defined|p75, p76|Holocene|Holocene|Of Sandfire Calcilutite. Consist of muddy red quatrz sand, muddy brown quartz sand (mud in the muddy sand is kaolinitic and/or calcilutaceous); sheet-like deposit occuring between red sand and calcilutite.||||||07-FEB-11
74634|Djugun Member|73213|5|Briefly described|958 Fig.3(a), 965 Fig.13|||||Sandfire Calcilutite.||Is overlain by Crab Creek and Lagrange, Calcilutite Members.|Muddy sand.|
23548|Dockrell Formation|23726|5|Briefly described|p8 Fig 2c|Eocene||Overlying unit Wilcox Formation. Underlying unit Lambert Formation. Geological Province: Carnarvon Basin.||||||
23548|Dockrell Formation|24390|5|Briefly described|p24 Table 6|||Geological Province: Northern Carnarvon Basin.||||||
23548|Dockrell Formation|40617|5|Briefly described|p16|||||||||
23548|Dockrell Formation|40800|2|Defined|p17|Late Paleocene|Early Paleocene|Early to Late Palaeocene.||||||07-NOV-08
23548|Dockrell Formation|41271|3|Fully described|p168|||||||||
23548|Dockrell Formation|41438|6|Mentioned|p110|||||||||
23548|Dockrell Formation|41439|6|Mentioned|p123|||||||||
23548|Dockrell Formation|41732|6|Mentioned|Fig.3|||||||||
23548|Dockrell Formation|42116|5|Briefly described|Fig.1 P6|||||||||
23548|Dockrell Formation|43712|6|Mentioned|Fig.10,p52||Paleocene|||||||
23548|Dockrell Formation|43724|6|Mentioned|Fig.15,p65||Paleocene|||||||
23548|Dockrell Formation|50085|5|Briefly described|p24 Tb. 6|Paleocene|Paleocene|Geological Province: Northern Carnarvon Basin (Barrow Sub-basin).||||||
23548|Dockrell Formation|61155|5|Briefly described|p15|Late Paleocene|Late Paleocene|Conformably overlies the Lambert Formation. Age: 62-59Ma. Max. thickness: 260m. Geological Province: Carnarvon Basin /offshore.||||||
23548|Dockrell Formation|62734|5|Briefly described|p1362 Fig. 2|Paleocene|Paleocene|Geological Province: Barrow Sub-basin.||||||01-SEP-08
23548|Dockrell Formation|62837|5|Briefly described|Stratigraphic columns|Eocene|Paleocene|Age: <60-55Ma. Geological Province: Dampier Sub-basin, Rankin Platform and Beagle Sub-basin.||||||01-MAR-10
23548|Dockrell Formation|63950|5|Briefly described|p336 Fig. 4|Paleocene|Paleocene|Overlies Lambert Formation; underlies Wilcox Formation. Geological Province: northern Carnarvon Basin.||||||23-JUN-14
23548|Dockrell Formation|67200|5|Briefly described|p8 fig 6, |Pliocene|Eocene|||||Overlies Lambert formation, overlain by Wilcox Formation|Crudely bedded limestone, sandstone and marl.|
23548|Dockrell Formation|67368|6|Mentioned|p209 Fig.4.|Paleocene|Paleocene|||||||
23548|Dockrell Formation|69692|6|Mentioned|p4|Paleocene|Paleocene|Northern Carnarvon Basin.||||Overlies Lambert Formation. Is overlain by Wilcox Formation.||
23548|Dockrell Formation|70066|5|Briefly described|Dampier: Fig.2. Exmouth: Fig.2|Thanetian|Selandian|See also Regional: Fig.6; p9. Northern Carnarvon Basin. Forms a top-seal for the Maitland gas accumulation in the Barrow Sub-basin.||||Overlies Lambert Formation. Is overlain by Wilcox Formation.||
23548|Dockrell Formation|70906|5|Briefly described|p757-758|Paleocene|Paleocene|Gorgon Platform.||||Overlies Withnell Formation. Is overlain by Wilcox Formation.||
24245|Doctors Creek Formation|36483|2|Defined|p71|Holocene|Holocene|Overlies, in large hollows of Christine Point Clay. Thickness: up to 12m. Geol.Prov: Canning Basin. Sand, shelly sand, sand/mud laminite, bioturbated mud, laminated mud, and conglomerate - mostly as lensoid, ribbon and/or wedge-shaped bodies.||||||07-AUG-07
24245|Doctors Creek Formation|37334|6|Mentioned|p199|||||||||
24245|Doctors Creek Formation|37615|5|Briefly described|Table 1|||||||||
24245|Doctors Creek Formation|38013|6|Mentioned|Fig.3|||||||||
74867|Dodonea Member|64643|5|Briefly described|p3 Fig. 2|Llandovery|Llandovery|Of Worral Formation?||||||
74867|Dodonea Member|65449|3|Fully described|p1,p6,p8-10,p27,p29,p31-33,p51-53,p59|Llandovery|Llandovery|New name, after Dodonea 1 well. Formerly an informal unit called 'lower carbonate member' (Lehmann, 1984) and assigned a type section 613-596m in Barbwire 1. Here the fully cored intervals 524.23-503.95m in Acacia 1 and 1015-1002m in Boab 1 are nominated as reference sections. Only known from the sub-surface. Average thickness is c.16m; maximum of 23.5m. Restricted to the Barbwire Terrace and adjacent areas. Represents a marine incursion across part of the Basin. Age from Ozarkodina hassi conodonts. Earlier reports of a Devonian ostracod and foraminifera fauna are not valid due to error in sample depth. Biostratigraphic data detailed.||Worral Formation.||Conformably overlies Sahara Formation. Is overlain by and intertongues with Elsa Sandstone Member.|A distinctive unit dominated by massive to weakly laminated and nodular carbonate, usually pale grey to beige dolomite, locally limestone; grading upwards to dolomitic or calcareous mudstone at the top; local minor sand.|
74053|Dombey Formation|13222|6|Mentioned|p229 Fig.2.|||||Unit in Kinmore Group.||||
74053|Dombey Formation|13242|2|Defined|p214 Fig. 2, p219|Late Permian|Late Permian|Of Hyland Bay Sub-gp (Kinmore Gp). Subdivided into 'defined' Upper and Lower Dombey Fm. Supersedes Dombey Member (Hyland Bay Formation). Geol.Province: Bonaparte Basin. Type section in Petrel 1, 3532 - 3549 m.|||||Bryozoan-rich limestone with shaly lower section passing up into massive limestone|21-DEC-12
74053|Dombey Formation|60386|6|Mentioned|p297|||Bonaparte Basin/Petrel Sub-basin. Limestone nearshore-shelf.||||||
74053|Dombey Formation|64690|5|Briefly described|p503, p504 Fig.2, p506 Tb.2, p517|Early Triassic|Late Permian|||Unit in Hyland Bay Sub-group.||Overlies Cape Hay Formation. Is overlain by Tern Formation.|Extensive offshore mudstones and carbonates.|
74053|Dombey Formation|64692|6|Mentioned|p522 Fig.2 |Late Permian|Late Permian|Bonaparte Basin.||Unit in Hyland Bay Sub-group.||Overlies Cape Hay Formation. Is overlain by Tern Formation.||
74053|Dombey Formation|67370|6|Mentioned|pp313-315, pp317-318.|Late Permian|Late Permian|Bonaparte Basin. At Fishburn-1 well, this unit is absent because of erosion. Contains a limestone marker bed.||||||
74053|Dombey Formation|69452|4|Described|p36:8, 15, 20|Wuchiapingian|Wuchiapingian|Bhatia et al. (1984); redefined in Mory (1988) and Gorter (1998). Petrel Sub-basin, Bonaparte Basin. Marine shelf deposits. Up to 30m thick. Offshore and onshore.||Hyland Bay Subgroup.||Unconformably overlies Cape Hay Formation. Is overlain unconformably by Tern Formation.|Laterally extensive; lower unit of limestone with shale intercalations, overlain by an upper unit of basal fine-grained sandstone, shale and marl below a second interval of limestone with shale interbeds. Limestone is bryozoan-rich.|12-JUL-16
74053|Dombey Formation|69454|5|Briefly described|p38:4|Wuchiapingian|Wuchiapingian|Petrel Sub-basin, Bonaparte Basin.||Hyland Bay Subgroup.||||12-JUL-16
74053|Dombey Formation|69653|6|Mentioned|p10|Lopingian|Lopingian|Petrel Sub-basin.||Hyland Bay Sub-group.||Overlies Cape Hay Formation. Is overlain by Tern Formation.||
74053|Dombey Formation|69673|6|Mentioned|p153 fig 125, p173|||||Hyland Bay Subgroup||Overlain by Tern Formation, overlies Cape Hay Formation||
74053|Dombey Formation|70061|5|Briefly described|Petrel Sub-basin Figs.2 & 3|Changhsingian|Wuchiapingian|See also Regional geology: Figs.6-8, p11. Vulcan: Fig.2. Shoreface to open marine biomicritic limestones form an intraformational seal.||Hyland Bay Subgroup.||Overlies Cape Hay Formation. Is overlain by Tern Formation.||12-JUL-16
74053|Dombey Formation|70774|5|Briefly described|p5 fig 3|Dzhulfian|Midian|Bonaparte Basin.||||||
74053|Dombey Formation|71623|4|Described|p349, 350, 354, 355, 356, 358, 359, 346|Wuchiapingian|Wuchiapingian|Bonaparte Basin.  At least 6 discrete cycles of limestone units separated by siliciclastic intervals in thicker intersections of Dombey Formation. Some palaeokarst evident. Significant gas shows. See also p343 and p352.||||Unconformably overlies Cape Hay Formation. Correlated with Upper Marine Beds, Hardman Formation. Unconformably overlain by Penguin Formation.|fine to medium-grained sparry limestone with comon shell fragments, bryozoans and crinoids. Sandy base in some places, shale in others. Some dolomite at top and bottom.|08-MAY-19
74053|Dombey Formation|72505|5|Briefly described|p890|Changhsingian|Wuchiapingian|Southern Bonaparte Basin. Correlated to the Dulhuntyispora parvithola zone.||||Overlies the Cape Hay Formation. Overlain by the Tern Formation.||12-MAR-20
23552|Dominic Shale|40837|2|Defined|p261, p275|Givetian|Givetian|Overlies Tandalgoo Formation.||||||27-JAN-10
23552|Dominic Shale|41169|6|Mentioned|p142|||||||||
23552|Dominic Shale|41215|5|Briefly described|p269|||Mention Fig.4||||||
23552|Dominic Shale|41730|6|Mentioned|Fig.3|||||||||
23552|Dominic Shale|63938|4|Described|p50|||Defined from Tappers Inlet 1, near Derby, NW Lennard Shelf. May correlate with Cadjebut Formation, therefore Devonian.||||||
23552|Dominic Shale|64643|4|Described|p31, p35|||Defined from Tappers Inlet 1, near Derby, NW Lennard Shelf. May correlate with Cadjebut Formation, therefore Devonian.||||||
23552|Dominic Shale|65301|6|Mentioned|p8 Fig. 5|||||||||
23552|Dominic Shale|65449|6|Mentioned|p51|||Overlies Worral Formation in Lovell's Pocket 1. Appears only as Dominic.||||Overlies Worral Formation.||
23552|Dominic Shale|66127|5|Briefly described|p441.|Middle Givetian|Middle Givetian|Pre-reef, subsurface strata in Canning Basin. Contains miospores from the lemuratua-magnificus zone.||||||31-JAN-14
23552|Dominic Shale|69182|6|Mentioned|Ch4 p30-p35, Ch4 p45|Carboniferous|Devonian|Canning Basin. Potential seal for the storage of carbon dioxde. ||||||
23552|Dominic Shale|69297|6|Mentioned|p337, p352|Frasnian|Givetian|Broome Platform of the Canning Basin. ||||Overlies the Tandalgoo Sandstone. Overlain by the Mellinjerie Limestone.||
77934|Donegal Komatiite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||2820 - 2711 Ma (inferred).||||Komatiite; olivine-spinifex texture and local well-developed cumulate zones; metamorphosed; locally silicified. Talc-chlorite(-carbonate) schist; minor tremolite-chlorite schist.|
77934|Donegal Komatiite|70326|3|Fully described|p336,338,341,343,346-8,350-1,353-4|Neoarchean|Neoarchean|Geological province: Agnew region, Ora Banda Domain, Kalgoorlie Terrane, Yilgarn Craton. Extrusive subaqueous komatiite flows, although alteration and deformation was focussed along the upper contact to produce cataclasites. Compositionally, the Donegal Komatiite is an uncontaminated Al-undepleted (Munro-type) komatiite (Arndt et al., 2008). Thickness: ~100 m. Top ~50 m observed in two drillholes and sporadic exposures on the western limb Agnew Anticline. Major and trace element geochemical analysis on Table 4 p342-346. See also p360,363-4.||||Overlain by Songvang Basalt. Underlain by Butchers Well Basalt.|Spinifex-orthocumulate LFA (aphyric komatiite, spinifex komatiite and ultrabasic cumulate, and lesser fragmental komatiite at the top. Subaqueous spinifex flows and cataclasites (fragmental komatiite) at top where deformation is concentrated.|
77934|Donegal Komatiite|71212|4|Described|intro p2, intro p3, p46, p47,  p223|||Yilgarn Craton. Between 250-300m thick. This unit is highly magnetic.  ||||Overlies the Butchers Well Basalt. Overlain by the Songvang Formation and the Hickies Bore Basalt.|Fine-grained and moderately or strongly foliated komatiite and high Mg basalts.|
77934|Donegal Komatiite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2820-2711 Ma (inferred)||||Komatiite; olivine-spinifex texture and local well-developed cumulate zones; metamorphosed; locally silicified; Talc-chlorite(-carbonate) schist; minor tremolite--chlorite schist/|
77934|Donegal Komatiite|73151|5|Briefly described|p3|Neoarchean|Neoarchean|Yilgarn Craton. Kalgoorlie Terrane, Agnew Greenstone Belt.||Kalgoorlie Group||Overlies Butchers Well Basalt, underlies Hickies Bore Basalt.|Komatiite.|
77934|Donegal Komatiite|73596|6|Mentioned|p1151-1152, 1156-1157, 1161-1163, 1167|||Lawlers Domain, Agnew-Wiluna Greenstone Belt. Deep-water mafic-ultramafic lava fields and feeder intrusions.||||Overlies Butchers Well Basalt. Is overlain by Hickies Bore Basalt.||
79244|Dongara Sequence|69297|6|Mentioned|p204, p207, p223, p236|||Perth Basin. ||||Unconformably overlain by the Kockatea Sequence.||
79244|Dongara Sequence|70097|5|Briefly described|p3, p4|Late Permian|Late Permian|Subsidence, offshore northern Perth Basin - Beagle Ridge and Abrolhos Sub-basin. Deposition of the upper Permian Dongara Sequence occurred during a thermal subsidence period. Transgressive facies filled incised valleys.||||||20-OCT-15
28510|Donnybrook Sandstone|23816|5|Briefly described|p246, 249|Early Cretaceous|Early Cretaceous|Geological Province: Perth Basin. Max. thickness: 60 m.||||||
28510|Donnybrook Sandstone|24160|6|Mentioned|p94|Cretaceous|Cretaceous|Perth Basin.||||||
28510|Donnybrook Sandstone|24410|5|Briefly described|p28|Cretaceous|Cretaceous|Yellow to grey, fine and medium-grained sandstone. Correlates with the Lower Cretaceous Warnbro Group (lower South Perth Shale and upper Leederville Formation). ||||||
28510|Donnybrook Sandstone|30146|6|Mentioned|p314|||Refers Balme (1956).||||||
28510|Donnybrook Sandstone|30188|2|Defined|p75|Cretaceous|Cretaceous|Refers to Saint-Smith(1912)||||||
28510|Donnybrook Sandstone|31562|6|Mentioned|p10|||Stratigraphic table||||||22-JUL-13
28510|Donnybrook Sandstone|33022|6|Mentioned|p261|||See also P265. Palaeomagnetism.||||||
28510|Donnybrook Sandstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
28510|Donnybrook Sandstone|35026|6|Mentioned|p331|||||||||
28510|Donnybrook Sandstone|35056|6|Mentioned|p90|||||||||
28510|Donnybrook Sandstone|36257|6|Mentioned|Table 2.1|||||||||
28510|Donnybrook Sandstone|36293|2|Defined|p175|Neocomian|Neocomian|||||||
28510|Donnybrook Sandstone|36890|3|Fully described|p249|||||||||
28510|Donnybrook Sandstone|37341|4|Described|p229|||||||||
28510|Donnybrook Sandstone|37344|6|Mentioned|p76|||||||||
28510|Donnybrook Sandstone|37350|6|Mentioned|Fig.1|||||||||
28510|Donnybrook Sandstone|37577|6|Mentioned|p53|||||||||
28510|Donnybrook Sandstone|40359|4|Described|p23|||||||||
28510|Donnybrook Sandstone|40360|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
28510|Donnybrook Sandstone|40928|6|Mentioned|p13|||||||||
28510|Donnybrook Sandstone|41780|5|Briefly described|p2|||||||||
28510|Donnybrook Sandstone|41912|6|Mentioned|p18|||||||||
28510|Donnybrook Sandstone|42711|6|Mentioned|p30|||Geological province: Perth Basin.  Approximately equivalent to Nakina Formation in the Collie Basin.||||||
28510|Donnybrook Sandstone|43038|5|Briefly described|p4|||||||||
28510|Donnybrook Sandstone|43189|5|Briefly described|Map Legend||Cretaceous|||||||
28510|Donnybrook Sandstone|43212|6|Mentioned|p6||Early Cretaceous|||||||
28510|Donnybrook Sandstone|44144|4|Described|p504 Tb.4-21, p516-517|Early Cretaceous|Early Cretaceous|Type Section: North of Donnybrook; 33o32'S 115o49'E.  60m thick fluvial or shoreline deposits; unfossiliferous. Maxicar beds are probably a facies of this Formation.||||Correlates with Warnbro Group.|Yellow to grey, fine- and medium-grained sandstone.|
28510|Donnybrook Sandstone|44303|14|Not recorded|p.9||Mesozoic|(I/50-5,9).||||||
28510|Donnybrook Sandstone|60556|5|Briefly described|p33|Permian||Permian||||||
28510|Donnybrook Sandstone|61273|5|Briefly described|p87|Cretaceous|Cretaceous|Used as dimension stone in the building industry. A commercial name as well as a stratigraphic name. Indurated fine- to medium-grained feldspathic and kaolinitic sandstone with colour variations from white to beige, and pink.||||||17-MAY-06
28510|Donnybrook Sandstone|64769|5|Briefly described|p7, p29, p30 Tb. 4, p32-33, p34 Fig. 22|Cretaceous|Cretaceous|Age: 125Ma. Thickness: 200m. Fine- to medium-grained, feldspathic sandstone that ranges through white to cream, pink, and pale brown. WA. Aslo on p131, p133 and p 132 Fig. 136. ||||||
28510|Donnybrook Sandstone|67861|6|Mentioned|p530|||Southern Perth Basin, and adjacent Yilgarn Craton. Correlated with Cretacous Nakina Formation.||||||
28510|Donnybrook Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, shale, conglomerate|
35655|Doon Doon breccia|23125|4|Described|Table.1, p389||Tertiary|||||||
32212|Double Bar Formation|23416|5|Briefly described|Map Legend|Archean|Archean|Of Coonterunah Group, Pilbara Craton||||||07-NOV-08
32212|Double Bar Formation|23755|4|Described|p18|Archean|Archean|See also page 17 Table 1. Of Coonterunah Group.||||||07-NOV-08
32212|Double Bar Formation|23783|5|Briefly described|p53|Archean|Archean|Of Coonterunah Group.||||||07-NOV-08
32212|Double Bar Formation|23784|5|Briefly described|p58|Archean|Archean|Of Coonterunah Group.||||||07-NOV-08
32212|Double Bar Formation|23813|5|Briefly described|p91 Tb. 1|Archean|Archean|Of the Coonterunah Group. Age: c.3.51Ga (U-Pb SHRIMP). Geological Province: Pilbara Craton.||||||11-APR-13
32212|Double Bar Formation|24025|4|Described|p9 Tb. 1|Archean|Archean|Of Coonterunah Group. Basalts and volcanogenic sedimentary rocks. Max. thickness: 2000 m. Geological Province: Pilbara Craton.||||||11-APR-13
32212|Double Bar Formation|24166|5|Briefly described|p9|Archean|Archean|Parent: Coonterunah Group.||||||07-NOV-08
32212|Double Bar Formation|24184|5|Briefly described|p699 Fig.3|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
32212|Double Bar Formation|24531|5|Briefly described|p5 Tb. 1|Archean|Archean|Of the Coonterunah Group (Pilbara Supergroup). Geological Province: Pilbara Craton.||||||11-APR-13
32212|Double Bar Formation|24550|5|Briefly described|p31 Tb. 3.1|Archean|Archean|Of the Coonterunah Group. Basalt, volcanogenic sediments. Age: 3508Ma. Geological Province: Pilbara Craton.||||||07-FEB-11
32212|Double Bar Formation|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Of the Talga Talga Subgroup (Warrawoona Group). Basalt and volcanogenic sedimentary rocks. Age: 3515Ma.||||||07-FEB-11
32212|Double Bar Formation|50379|5|Briefly described|Map Legend|Archean|Archean|Of Coonterunah Group (Pilbara Supergroup). Geological Province: Pilbara Craton.||||||07-NOV-08
32212|Double Bar Formation|60112|5|Briefly described|p108-110, p113 Tb.1, p115.  ||||3515 Ma.|Unit in Coonterunah Group.||Intruded by North Pole Monzogranite. Overlain by the Dresser Formation and the Mount Ada Basalt.|Metabasalts.|
32212|Double Bar Formation|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Geological Province: eastern Pilbara Craton.||||||07-NOV-08
32212|Double Bar Formation|61266|4|Described|p56-57 FIg.1|Archean|Archean|Of the Coonterunah Group. Overlies the Coucal Formation. Max. thickness: 2 km. Massive to pillowed tholeiitic basalts, local mafic tuffaceous rocks and rare chert. Geological Province: Pilbara Craton. See also p58 Tb.1.||||||11-APR-13
32212|Double Bar Formation|61579|5|Briefly described|p58 Fig. 2|Archean|Archean|Of the Coonterunah Group.||||||07-NOV-08
32212|Double Bar Formation|63441|5|Briefly described|p4 Tb. 1|Archean|Archean|Of Coonterunah Subgroup (Warrawoona Group, Pilbara Supergroup).||||||07-FEB-11
32212|Double Bar Formation|63538|5|Briefly described|p8, p6 Fig. 3|Archean|Archean|Upper unit of Coonterunah Subgroup. Underlain by Coucal Formation. Geological Province: Pilbara Craton.||||||19-APR-13
32212|Double Bar Formation|64328|5|Briefly described|p56 Tb. 1|||Of Talga Talga Subgroup (Warrawoona Group). Basalt.||||||07-FEB-11
32212|Double Bar Formation|64405|5|Briefly described|p4|Archean|Archean|Name inferred from Double Bar only in Figure 3. Of the Warrawoona Group (De Grey Supergroup).||||||07-FEB-11
32212|Double Bar Formation|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in upper Coonterunah Subgroup. Age shown as <3498 Ma. Basalt, massive or pillowed; locally schistose; metamorphosed.||||||
32212|Double Bar Formation|66217|6|Mentioned|p14. |||Does not crop out in Coongan map sheet area.||Unit in Coonterunah Subgroup.||||10-JUN-20
32212|Double Bar Formation|66664|6|Mentioned|p7.||||||||Metabasalt.|
32212|Double Bar Formation|66745|5|Briefly described|pp53-54.|Paleoarchean|Paleoarchean|||Unit in Coonterunah Subgroup.||Overlies Coucal Formation.|Basalt.|
32212|Double Bar Formation|67197|5|Briefly described|p4-5, p18, p25|Paleoarchean|Paleoarchean|East Pilbara Terrane.|3498 Ma.|Coonterunah Subgroup.||||
32212|Double Bar Formation|67201|5|Briefly described|p7 Fig.4, p12 Tb.1|||In northern Pilbara Craton, East Pilbara Terrane.||Coonterunah Subgroup||||
32212|Double Bar Formation|67269|5|Briefly described|p5-6|Paleoarchean|Paleoarchean|||Coonterunah Subgroup.|||Basalt.|
32212|Double Bar Formation|67270|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Coonterunah Subgroup.||||
32212|Double Bar Formation|67668|6|Mentioned|Fig. 2; p. 153||Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Coonterunah Subgroup of the Warrawoona Group||Overlies the Coucal Formation.|Mafic volcanic rocks.|17-SEP-14
32212|Double Bar Formation|68035|5|Briefly described|p288 Fig 4||Paleoarchean|Warrawoona Group, Pilbara Supergroup, East Pilbara Terrane.||Of Coonterunah Subgroup||Overlies Coucal Formation.|Basalt.|
32212|Double Bar Formation|68280|6|Mentioned|p4|||||Coonterunah Subgroup||Overlies Coucal Formation|Basalt.|
32212|Double Bar Formation|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Coonterunah Subgroup.|||Mafic schist derived from basalt.|23-SEP-13
32212|Double Bar Formation|68284|5|Briefly described|p7|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Coonterunah Subgroup.||Overlies Coucal Formation.||
32212|Double Bar Formation|69013|6|Mentioned|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Unit in Warrawoona Group.||||
32212|Double Bar Formation|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Includes 3 unnamed sub-units mapped separately.||Of the Coonterunah Subgroup.|||Basalt, massive or pillowed, locally schistose, metamorphosed; silicified amphibolite and amphibolite schist, medium grained and variably foliated; silicified metamafic volcanic rock; mafic schist derived from basalt.|02-MAY-14
32212|Double Bar Formation|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Coonterunah Subgroup|||Basalt; massive or pillowed; locally schistose; metamorphosed. Silicified amphibolite and amphibolite schist, metadolerite, silicified metamafic volcanic rock, mafic schist derived from basalt.|
32212|Double Bar Formation|69301|5|Briefly described|p5 Fig.3, p9 Tb.1|||Pilbara Craton. East Pilbara Terrane.||Coonterunah Subgroup|||Basalt.|
32212|Double Bar Formation|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|3515-3490 Ma (inferred)|Unit of Coonterunah Subgroup.|||Basalt, mafic schist derived from basalt, silicified amphibolite and  amphibolite schist, metadolerite, silicified metamorphosed mafic volcanic rock.|
32212|Double Bar Formation|70022|6|Mentioned|p115|||East Pilbara Terrane.||Coonterunah Subgroup.||||
32212|Double Bar Formation|70775|5|Briefly described|p12|||East Pilbara.||Warrawoona Group||Overlies the Coucal Formation. Overlain by the North Star Basalt.||
32212|Double Bar Formation|70884|5|Briefly described|p123|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Coonterunah Subgroup.||Overlain by  North Star Basalt/Talga Talga Subgroup. Underlain by Coucal Formation.||
32212|Double Bar Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Warrawoona  Large Igneous Province.||Coonterunah Subgroup|||Basalt; massive or pillowed; locally schistose; metamorphosed.|
32212|Double Bar Formation|72064|5|Briefly described|p66-67|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|3498 Ma|Unit of Warrawoona Group.||Overlain by North Star Basalt. Unconformably overlain by the Strelley Pool Formation. Underlain by Coucal Formation.||28-JAN-20
32212|Double Bar Formation|72251|5|Briefly described|p54|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unt of Coonterunah Subgroup.||Uppermost unit of Coonterunah Subgroup. Overlain by North Star Basalt. Underlain by Coucal Formation.||
32212|Double Bar Formation|72668|6|Mentioned|p4-6|||East Pilbara Terrane.||Coonterunah Subgroup||Overlies the Coucal Formation.||
32212|Double Bar Formation|73598|6|Mentioned|p1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Coonterunah Subgroup.||Overlies Coucal Formation. Is overlain by North Star Basalt.||
24254|Double Nob Formation|36483|2|Defined|p69|Pleistocene|Pleistocene|Conformably overlies Airport Creek Fm; underlies Christine Point Clay. Thickness: 1m. Geol.Prov: Canning Basin. A soil, comprising homogeneous, dark grey, muddy sand cemented by low magnesian calcite into graine-sized nodules; +medium+coarse sand grains.||||||07-AUG-07
24254|Double Nob Formation|37615|5|Briefly described|Table 1|||||||||
24254|Double Nob Formation|38013|6|Mentioned|Fig.3|||||||||
24927|Dougalls Suite|22526|6|Mentioned|Fig2 P681, Fig3||Orosirian|||||||
24927|Dougalls Suite|22547|6|Mentioned|p13|||||||||
24927|Dougalls Suite|24197|4|Described|p20|Paleoproterozoic|Paleoproterozoic|Incl: Dougalls Granitoid, Corkwood, Dead Finish, Monkey Yard + Reedy Creek Tonalites - as series of sheets into Tickalara Metamorphics. Age: ~1850Ma. Predominantly tonalite, trondhjemite leucogranite. In East Kimberley region. Eg.of Sally Downs Assocn.||||||07-FEB-11
24927|Dougalls Suite|41977|4|Described|p474|||||||||
24927|Dougalls Suite|50437|5|Briefly described|p1.6, 5.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Age: 1850Ma. Geological Province: Kimberley Region.||||||07-NOV-08
24927|Dougalls Suite|63866|5|Briefly described|p131|||Central Zone, Halls Creek Orogen.|||||Tonalite, quartz diorite and gabbro.|
24927|Dougalls Suite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.|||Includes Black Duck Tonalite, Dougalls Tonalite, and unnamed unit.||Foliated metatonalite and minor metagranodiorite with abundant inclusions of amphibolite and mafic granulite; interlayered mafic granulite and amphibolite.|30-JUL-15
24927|Dougalls Suite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||||Includes Black Duck Tonalite, Dougalls Tonalite,||Dioritic, quartz dioritic, and gabbroic granulite, and amphibolite; intimately veined by metatonalite.|
24927|Dougalls Suite|69585|6|Mentioned|p4|Orosirian|Orosirian|Central Lamboo Province.||||||
24927|Dougalls Suite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Central Zone. See 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|1849-1849 Ma (Inferred)||Includes Black Duck Tonalite, Dougalls Tonalite.||Foliated metatonalite and minor metagranodiorite with abundant inclusions of amphibolite and mafic granulite; interlayered mafic granulite and amphibolite|
24927|Dougalls Suite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv.|1849 Ma||||Dioritic, quartz dioritic, gabbroic granulite and amphibolite veined by metatonalite.|
24927|Dougalls Suite|70812|4|Described|p3, p6-p7, p13, p24-p25, p27|Orosirian|Orosirian|Central Zone of the Halls Creek Orogen, Lamboo Province. Prospective for Cu-fertile porphyries on the basis of geochemistry. Metamorphosed at high temperature, low pressure amphibolite to granulite facies at 1865-1856 and 1850-1845 Ma. Mineralisation is described.|c. 1865 Ma|||Intrudes the Tickalara Metamorphics.|Tonalite, trondhjemite and quartz diorite.|
24927|Dougalls Suite|70851|4|Described|p3-p5, p18|Paleoproterozoic|Paleoproterozoic|Central Zone, Lamboo Province. Deformed and metamorphosed to amphibolite and granulite facies at 1850-1845 Ma during the Hooper Orogeny.|c. 1865 Ma||Includes the Dougalls Tonalite.||Tonalite, trondhemite and quartz diorite.|23-MAR-23
24927|Dougalls Suite|71113|5|Briefly described|p98,100|Orosirian|Orosirian|Geological province: Central Zone, Lamboo Province, Halls Creek Orogen. Used interchangeably in text with Dougalls Suite. Intruded into, and metamorphosed Tickalara Metamorphics at 1850 Ma in an island arc (Sheppard et al., 2001) or convergent continental margin setting (Sheppard et al., 1997, 2001).|1850 Ma||||Tonalite, trondhjemite and quartz diorite sheets.|
24927|Dougalls Suite|71140|6|Mentioned|p98, 100|Orosirian|Orosirian|Central Zone, Lamboo Province, Halls Creek Orogen. Either an island arc or convergent continental margin setting.|||Dougalls Tonalite.|Intrudes and metamorphoses Tickalara Metamorphics.|Tonalite, trondhjemite and quartz diorite sheets.|
24927|Dougalls Suite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|1849 Ma (inferred)||Includes Black Duck Tonalite, Tickalara Metamorphics.||Foliated metatonalite and minor metagranodiorite with abundant inclusions of amphibolite and mafic granulite; interlayered mafic granulite and amphibolite|
24927|Dougalls Suite|71397|6|Mentioned|p5|Orosirian|Orosirian|Geological province: Central Zone, Lamboo Province, Halls Creek Orogen.||||||
24927|Dougalls Suite|71873|5|Briefly described|p442-444|Orosirian|Orosirian|Geological province: Lamboo Province. Coeval with Koongie Park volcanics. Deformed by Hooper Orogeny c. 1860 Ma. |1850 Ma|||||
24927|Dougalls Suite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Central Zone, Halls Creek Orogen.|||||Foliated metatonalite and minor metagranodiorite with abundant inclusions of amphibolite and mafic granulite; interlayered mafic granulite and amphibolite.|
31881|Dougalls Tonalite|22547|6|Mentioned|p13|||Of Dougalls Suite.||||||14-NOV-06
31881|Dougalls Tonalite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of Dougalls suite.  Age c. 1850 Ma||||||07-NOV-08
31881|Dougalls Tonalite|23323|5|Briefly described|p456 Table 1|Orosirian|Orosirian|Age: 1849 +/- 3 Ma.||||||07-FEB-07
31881|Dougalls Tonalite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tickalara Metamorphics (Lamboo Complex).  Age: 1865-1850Ma.||||||07-NOV-08
31881|Dougalls Tonalite|43853|5|Briefly described|Map Legend||Proterozoic|part of Tickalara Metamorphics, Lamboo Complex.||||||
31881|Dougalls Tonalite|43855|5|Briefly described|Map Legend||Proterozoic|||||||
31881|Dougalls Tonalite|44155|5|Briefly described|p239 Tb.3-3, p248 Tb.3-8|||East Kimberley. Mis-spelt as Dougals Tonalite. Multiply deformed.||Lamboo Complex||Intrudes Melon Patch Granite.|Foliated porphyritic biotite-hornblende tonalite.|
31881|Dougalls Tonalite|44230|5|Briefly described|Map Legend||Proterozoic|||||||
31881|Dougalls Tonalite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31881|Dougalls Tonalite|50437|5|Briefly described|p1.6, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Dougalls Suite. Age: 1849 +/- 3Ma (SHRIMP).||||||11-JUN-14
31881|Dougalls Tonalite|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Tickalara Metamorphics. Age: c. 1850Ma. Foliated and metamorphosed hypersthene-hornblende-biotite tonalite; abundant pyroxene amphibolite and country rock inclusions.||||||03-NOV-04
31881|Dougalls Tonalite|60724|6|Mentioned|p20|||Same as Dougalls Granitoid suite?||||||
31881|Dougalls Tonalite|63866|5|Briefly described|p131, p138|||Central Zone, Halls Creek Orogen.|c. 1849 Ma|||Intrudes the Tickalara Metamorphics.||
31881|Dougalls Tonalite|66845|4|Described|p538 Fig.4, p539 Tb.1, p540-1|||The Dougalls Tonalite and Fletcher Creek Monzogranite have the same crystallisation age, and are part of a widespread magmatic event in the Central zone of the Lamboo Complex at c. 1850 Ma. |20 analyses, zircon recrys. 1849+/-3Ma SHRIMP U-Pb|Dougalls suite|||Hypersthene granulite|30-JUL-15
31881|Dougalls Tonalite|66846|5|Briefly described|p558 Table 4|Orosirian|Orosirian|Age probably from U-Pb SHRIMP dating of zircon (see p547). |~1849|Of Dougalls suite.||||
31881|Dougalls Tonalite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Data from OZCHRON1. Comment: 'Twenty concordant to sub-concordant data points define this magmatic age for the hypersthene-bearing granulite. This age also dates the peak of high-grade metamorphism, and probably the D2 deformation as the intrusion is syn-D2.'|crystallisation age 1849+/-3 Ma U/Pb SHRIMP|Dougalls Suite|||Foliated hornblende-biotite(-hypersthene) metatonalite and metagranodiorite; locally contains garnet or epidote; inclusions of amphibolite, metadiorite, and country rock|30-JUL-15
31881|Dougalls Tonalite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv, GA_geochron.csv. |1849-2258 Ma|Dougalls Suite|||Foliated hornblende--biotite(--hypersthene) metatonalite and metagranodiorite; locally contains garnet or epidote; inclusions of amphibolite, mafic granulite, metadiorite, and country rock.|
31881|Dougalls Tonalite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Central Zone.|1849-1849 Ma (Isotopic)|Unit of Dougalls Suite.|||Foliated hornblende-biotite(-hypersthene) metatonalite and metagranodiorite; locally contains garnet or epidote; inclusions of amphibolite, metadiorite, and country rock|
31881|Dougalls Tonalite|70154|6|Mentioned|GA_geochron.csv|||||||||
31881|Dougalls Tonalite|70731|6|Mentioned|p272-273|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. Median density: 3070 kg/m3.||||||
31881|Dougalls Tonalite|70851|5|Briefly described|p11-p12|||Rock properties are provided.||Dougalls Suite||||
31881|Dougalls Tonalite|71113|6|Mentioned|p98|||Geological province: Central Zone, Lamboo Province, Halls Creek Orogen. Used interchangeably in text with Dougalls Tonalite.||||||
31881|Dougalls Tonalite|71140|6|Mentioned|p98|Orosirian|Orosirian|Central Zone, Lamboo Province, Halls Creek Orogen.|c.1850 Ma.|Dougalls Suite.||||
31881|Dougalls Tonalite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1849+\-3 Ma (isotopic)|Unit of Tickalara Metamorphics.|||Foliated hornblende-biotite(-hypersthene) metatonalite and metagranodiorite; locally contains garnet or epidote; inclusions of amphibolite, metadiorite, and country rock|
31881|Dougalls Tonalite|72437|6|Mentioned|p6, p45-46|||Ogasawara (1988) presented major and trace-element analyses including REE for four samples of this unit.||||||
31270|Douri Sandstone|22496|2|Defined|p11||Neoproterozoic|Of the Albert Edward Group.  Conformably overlies the Boonall Dolomite; inferred to be overlain by concealed Timperley Shale.  Geological Province: Wolfe Basin.||||||16-AUG-04
31270|Douri Sandstone|22777|5|Briefly described|Map|||Albert Edward Group, Wolfe Basin||||||
31270|Douri Sandstone|23621|2|Defined|P52 Appendix|Neoproterozoic|Neoproterozoic|See also page 34, 9 table 1. Type section included. Previously mapped as part of Mount Forster Sandstone. Of Albert Edward Group. Overlying unit Timperley Shale. Underlying unit Boonall Dolomite. Wolfe Basin. Max. thickness: 150 m.||||||
31270|Douri Sandstone|23622|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Albert Edward Group. Geological Province: Wolfe Basin.||||||
31270|Douri Sandstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Wolfe Creek Basin||Albert Edward Group|||Lithic sandstone; micaceous siltstone, shale; minor dolomitic beds|30-JUL-15
31270|Douri Sandstone|69165|5|Briefly described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran||||||Lithic sandstone; micaceous siltstone, shale; minor dolomitic beds.|
31270|Douri Sandstone|69634|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1.|635-541 Ma (Inferred)|Unit of Albert Edward Group.|||Lithic sandstone; micaceous siltstone, shale; minor dolomitic beds|
31270|Douri Sandstone|70154|6|Mentioned|100k_interpgeop_lut.csv|Fortunian|Ediacaran||541-635 Ma|Albert Edward Group||||
31270|Douri Sandstone|71267|4|Described|GEOL_LUT_CSV files|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|635-541 Ma (inferred)|Unit of Albert Edward Group.|||Lithic sandstone; micaceous siltstone, shale; minor dolomitic beds|
23558|Doyle Dam Granodiorite|41786|4|Described|p333|||||||||
23558|Doyle Dam Granodiorite|42740|5|Briefly described|map legend|Archean||||||||07-NOV-08
23558|Doyle Dam Granodiorite|43125|4|Described|p9, and map insert|Archean|Archean|||||||03-MAR-10
23558|Doyle Dam Granodiorite|43232|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
23558|Doyle Dam Granodiorite|60076|5|Briefly described|p45 App. 1|||[Aggdd]   K-feldspar-phyric, massive to weakly foliated granodiorite.||||||
23558|Doyle Dam Granodiorite|65204|6|Mentioned|p19 Tbl.4.|Neoarchean||0.5-5mm grains; equigranular||||||
23558|Doyle Dam Granodiorite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|K-feldspar-phyric granodiorite; massive to weakly foliated; discordant to greenstones.||||||07-FEB-11
23558|Doyle Dam Granodiorite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Post-D2 to syn-D3, K-feldspar-phyric granodiorite; massive to weakly foliated; discordant to greenstones.|05-AUG-15
23558|Doyle Dam Granodiorite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Post-D2 to syn-D3, K-feldspar-phyric granodiorite; massive to weakly foliated; discordant to greenstones.|
23558|Doyle Dam Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite|
23558|Doyle Dam Granodiorite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|3010-2600 Ma (inferred)||||K-feldspar-phyric granodiorite; massive to weakly foliated|
36957|Dresser Formation|23416|5|Briefly described|Map Legend|Archean|Archean|Of Talga Talga Subgroup, Pilbara Craton.||||||07-NOV-08
36957|Dresser Formation|23755|4|Described|p19|Archean|Archean|See also page 17 table 1. Of Warrawoona Group.||||||07-NOV-08
36957|Dresser Formation|23783|5|Briefly described|p14|Archean|Archean|Of Talga Talga Subgroup.  Age: 3490Ma.  See also p53.||||||07-NOV-08
36957|Dresser Formation|24025|4|Described|p9 Tb. 1|Archean|Archean|Of Talga Talga Subgroup. Blue, black and white layered chert, barite, carbonate, and mafic volcanic rocks; stromatolites. Max. Thickness: 1500 m. Geological Province: Pilbara Craton.||||||11-APR-13
36957|Dresser Formation|24110|5|Briefly described|Plate 1|Archean|Archean|Of the Warrawoona Group. Geological Province: Pilbara Craton.||||||11-APR-13
36957|Dresser Formation|24184|5|Briefly described|p699, 701, 705|Archean|Archean|Parent: Talga Talga Subgroup. Geological Province: Pilbara Craton. Age: ca.3490Ma. Formerly correlated as part of Towers Formation, now a distinct unit (Van Kranendonk 2000).||||||07-NOV-08
36957|Dresser Formation|24185|5|Briefly described|p740, p751|Archean|Archean|Age: ca. 3490 Ma (Thorpe et al, 1992). Geological Province: Pilbara Craton.||||||07-NOV-08
36957|Dresser Formation|24531|5|Briefly described|p5 Tb. 1|Archean|Archean|Of the Talga Talga Subgroup (Warrawoona Group).  Age: c. 3490Ma. Geological Province: Pilbara Craton.||||||11-APR-13
36957|Dresser Formation|24550|5|Briefly described|p31 Tb. 3.1|Archean|Archean|Of the Talga Talga Subgroup (Warrawoona Group). Stromatolitic barite-chert. Age: ca 3490Ma. Geological Province: Pilbara Craton.||||||07-FEB-11
36957|Dresser Formation|60112|5|Briefly described|p108-109, p112. ||||3490 Ma|Unit in Warrawoona Group.||Overlies the Double Bar Formation. Is overlain by Duffer Formation.|Basalt.|
36957|Dresser Formation|60636|5|Briefly described|p86, p99|Archean|Archean|Comprises silicified sedimentary cherts interbedded with pillow basalts; includes chert-barite veins up to 10m wide. Age: ~3.49Ga.||||||07-FEB-11
36957|Dresser Formation|61111|6|Mentioned|p96 Fig.2|||Only chert shown.||||||
36957|Dresser Formation|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Geological Province: eastern Pilbara Craton.||||||07-NOV-08
36957|Dresser Formation|61256|5|Briefly described|p339|Archean|Archean|A shallow water hydrothermal system; contains stromatolites.  Age: ca. 3.49Ga.  Geological Province: in the North Pole Dome of the Pilbara Craton. See also p341, p342-3, p348.||||||07-NOV-08
36957|Dresser Formation|61257|5|Briefly described|p354 Fig. 1|Archean|Archean|Contains the Dresser Chert - probably an informal reference to a chert layer in the formation.  Geological Province: North Pole Dome of the Pilbara Craton.||||||07-NOV-08
36957|Dresser Formation|61579|5|Briefly described|p58 Fig. 2|Archean|Archean|Of the Warrawoona Group.||||||07-NOV-08
36957|Dresser Formation|62979|5|Briefly described|p212 Fig. 1, p213|Archean|Archean|Of the Warrawoona Group. Contains the Dresser Chert.  Age: 3490 Ma. Geological Province: Pilbara Craton.||||||11-APR-13
36957|Dresser Formation|63245|5|Briefly described|p4 Fig. 1, p5 Fig. 2|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Age: <3490Ma. Geological Province: Pilbara Craton. Contains hydrothermal chert-barite units with putative stromatolites and microfossils.||||||07-NOV-08
36957|Dresser Formation|63441|5|Briefly described|p4 Tb. 1, p19|Archean|Archean|Of Coonterunah Subgroup (Warrawoona Group, Pilbara Supergroup). Age: 3525+/-2Ma. Overlain by either Kelly Group unconformably, or disconformably Talga Talga or Coongan Subgroup rocks. Type area is in the East Strelley greenstone belt.||||||07-FEB-11
36957|Dresser Formation|63538|5|Briefly described|p6 Fig. 3|Archean|Archean|Of Coonterunah Subgroup. Geological Province: Pilbara Craton.||||||19-APR-13
36957|Dresser Formation|63649|5|Briefly described|p201|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Age: 3.49Ga. Geological Province: Pilbara Craton.||||||07-FEB-11
36957|Dresser Formation|64328|5|Briefly described|p56 Tb. 1|||Of Talga Talga Subgroup (Warrawoona Group). Chert, basalt.||||||07-FEB-11
36957|Dresser Formation|64405|5|Briefly described|p2 Fig. 1, p19|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Age: 3480Ma. Geological province: East Pilbara Terrane.||||||07-FEB-11
36957|Dresser Formation|64580|4|Described|map legend||Paleoarchean|Of Talga Talga Subgroup. Chert and mafic volcanic rock; metamorphosed.||||||22-OCT-08
36957|Dresser Formation|64747|4|Described|p93-123|Paleoarchean|Paleoarchean|North Pole Dome, Pilbara Craton. Putative signs of life are present as stratiform, columnar, domical, and coniform stromatolitic laminates. 4-60m thick. A Pb-Pb isochron age of 3490 Ma was obtained for galena in barite (Thorpe et al., 1992). Younger U-Pb SHRIMP zircon age is of volcaniclastic tuff unit near top. Absence of Duffer Formation detrital zircons implies deposition of Dresser Formation before 3470 Ma.|3481.0 +/- 3.6 Ma (Van Kranendonk et al. 2008).|Warrawoona Group.||Overlain by Strelley Pool Chert (unconformably).|Basal fossiliferous bedded grey, white, black and locally red chert with thick, coarsely crystalline barite unit, conglomerate, sandstone, carbonate and stromatolitic laminates; overlain by pillowed komatiitic basalt, greenschist metamorphosed.|
36957|Dresser Formation|65827|6|Mentioned|p47|||Hosts hydrothermal chert and barite deposits.||||||21-JAN-22
36957|Dresser Formation|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Aged c. 3481 Ma. Chert and mafic volcanic rock; metamorphosed.||||||
36957|Dresser Formation|66217|4|Described|p14, p15. |Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Deposited in a felsic volcanic caldera; hosts massive hydrothermal barite mineralisation at the North Pole Dome caldera. Restricted to the Panorama greenstone belt; forms a lateral equivalent to McPhee Formation.|3481 +/- 2 Ma (Van Kranendonk et al. 2008).|Unit in Talga Talga Subgroup.||Is overlain conformably by Mount Ada Basalt.|Grey and white (locally jaspilitic) layered metachert; finely laminated sulfides with stromatolitic textures; minor bedded carbonate, coarse polymictic breccia horizons, and sandstone.|
36957|Dresser Formation|66664|5|Briefly described|p3, p4, p12 Fig.12. |Archean|Archean|East Pilbara Terrane. Probably oldest fossil evidence of life on Earth preserved in stromatolite mats and sandstone in Buick State Geoheritage Reserve.||Unit in Talga Talga Subgroup.|||Basalt and chert.|
36957|Dresser Formation|66745|3|Fully described|p51, pp53-54, pp56-57.|Paleoarchean|Paleoarchean|Re-assigned to Talga Talga Subgroup following revised geochronology and a new correlation with McPhee Formation. Crustal extension, with hydrothermal activity in thermal lakes (stromatolites) in caldera setting. Base metal mineralization.|<3481-3477 Ma.|Unit in Talga Talga Subgroup.||Overlies North Star Basalt. Is disconformably overlain by Mount Ada Basalt.|Basalt, chert, carbonate rocks; minor felsic volcaniclastic rocks; also hydrothermal barite, evaporites and stromatolites.|09-OCT-15
36957|Dresser Formation|67130|5|Briefly described|p16, p17, p62|Paleoarchean|Paleoarchean|Deposited under tectonically active setting, indicated by lateral facies variations, olistostrome breccia and internal erosional unconformities.  Contains the worlds oldest stromatolites. See also  p64 fig 62, p65 fig 63, p68, p69. |3477 Ma, 3481 +/- 2 Ma (SHRIMP U/Pb)|Warrawoona Group||Overlies North Star Basalt, overlain by Mount Ada Basalt|Chert and barite horizons interbedded with pillow basalts and dolerite. Silicified carbonate rocks with stromatolites.|
36957|Dresser Formation|67197|5|Briefly described|p3-4|Paleoarchean|Paleoarchean|East Pilbara Terrane.|3477 Ma.|Talga Talga Subgroup.||||
36957|Dresser Formation|67201|4|Described|p7 Fig.4, p12 Tb.1|||In northern Pilbara Craton, East Pilbara Terrane. Shown as McPhee and Dresser Fm.|c. 3480 Ma|Talga Talga Subgroup||||
36957|Dresser Formation|67269|5|Briefly described|p3, p6 Fig.3|Paleoarchean|Paleoarchean|Contains stromatolites older than those in the Strelley Pool Formation at the Trendall Reserve.|<3481-3477 Ma.|||Overlies North Star Basalt. Is overlain by Mount Ada Basalt.||
36957|Dresser Formation|67270|5|Briefly described|p3-4|Paleoarchean|Paleoarchean|East Pilbara Terrane.|<3481-3477 Ma.|Talga Talga Subgroup.||Overlies Talga Talga Subgroup. Is overlain by Coongan Subgroup.||
36957|Dresser Formation|67668|5|Briefly described|Fig. 2-5; p154,156,160-161,163; Tb.1 ||Paleoarchean|East Pilbara Terrane, Pilbara Craton. Geographically restricted to only a ~25 km2 area around the North Pole Dome. Controversial evidence of possible early life is reviewed - includes putative stromatolites and microfossils.|3490 Ma|Warrawoona Group|||Complex volcano-sedimentary unit consisting of bedded chert, sulfate, carbonate and jasper, together with pillow basalt and dolerite. Up to four sedimentary chert-sulfate-carbonate members.|
36957|Dresser Formation|68035|5|Briefly described|p293, 294, p288 fig 4|Paleoarchean|Paleoarchean|Warrawoona Group, Pilbara Supergroup, East Pilbara Terrane. Includes stromatolites, microbial mats or microfossils deposited around hot springs or hydrothermal vents. Includes barite ore. Shown as McPhee and Dresser Formations (<3481-3477 Ma), in Fig 4.|3.48 Ga|Of Talga Talga Subgroup.||Overlies North Star Basalt? Disconformably overlain by Mount Ada Basalt.||
36957|Dresser Formation|68280|4|Described|p2, p4, p6-p12, p16, p17|Paleoarchean|Paleoarchean||3481 +/- 2 Ma (SHRIMP)|Talga Talga Subgroup||Disconformably overlain by Mount Ada Basalt, overlies North Star Basalt|Chert and barite interbedded with pillow basalts and dolerite. Komatiites and siliciclastic rocks. Stromatolites present throughout|
36957|Dresser Formation|68284|5|Briefly described|p2, 5, 7, 20|Paleoarchean|Paleoarchean|North Pole Dome, Pilbara region. Contains probably the oldest known stromatolites.|c.3481 Ma.|Talga Talga Subgroup (Warrawoona Group).||Overlies North Star Basalt. Is overlain by Apex or Mount Ada Basalt.|Contains domical stromatolites.|
36957|Dresser Formation|69015|5|Briefly described|Map Legend|Archean|Archean|East Pilbara Terrane, Pilbara Craton. Mapped as 3 unnamed sub-units.||Of the Talga Talga Subgroup.|||Hydrothermal black, blue-black, or grey chert in dykes and sills; layered chert, includes silicified evaporite deposits and volcanic sandstone, locally stromatolitic; pillowed komatiitic basalt and minor basalt, metamorphosed.|02-MAY-14
36957|Dresser Formation|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Age derived from sample of felsic volcaniclastic sandstone (180070.1.pdf) and is the maximum age for deposition for the sandstone.|3481 +/- 3 Ma (SHRIMP)|Talga Talga Subgroup|||Hydrothermal chert, layered chert; includes silicified evaporite deposits and volcanic sandstone. Pillowed komatiitic basalt and minor tholeiitic basalt; metamorphosed.|
36957|Dresser Formation|69185|4|Described|GEOL_LUT_CSV files||Paleoarchean|Geological province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.||Unit of Talga Talga Subgroup.|||Chert and mafic volcanic rock; metamorphosed|
36957|Dresser Formation|69301|4|Described|p5 Fig.3, p9 Tb.1, p11, p20, p22-23|||Pilbara Craton. East Pilbara Terrane. Shown as McPhee and Dresser Fm. Age: <3481-3477 Ma McPhee and Dresser Formations.|3.48 Ga. See comments|Talga Talga Subgroup||Disconformity at top of McPhee Formation and Dresser Formation.|Komatiite, siliciclastic rocks. Deposition included widespread shallow-water hydrothermal settings, and possibly even evaporite deposits.|
36957|Dresser Formation|69569|6|Mentioned|p285 Fig.1, p287-288|||East Pilbara Terrane.||Warrawoona Group.||||
36957|Dresser Formation|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA 180070 (volcaniclastic sandstone) yielded a possible maximum depositional age of 3481+\-3 Ma for the sandstone (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|3481-3477 Ma (inferred)|Unit of Talga Talga Subgroup.|||Hydrothermal chert; in dykes and sills; local barite veins; layered chert; includes silicified evaporite deposits and volcanic sandstone; locally stromatolitic; metamorphosed; pillowed komatiitic and tholeiitic basalt, metamorphosed.|
36957|Dresser Formation|69989|5|Briefly described|p24-34|Paleoarchean|Paleoarchean|Pilbara Craton. Much of the original mineralogy replaced by silica, barite, pyrite, hematite and kaolinite due to contemporaneous volcanic hydrothermal fluids. Multiple S isotope data tabulated, discussed.|3481 Ma.|Warrawoona Group.||Overlies Coonterunah Subgroup.|Komatiitic basalts, black chert veins, shallow-water carbonates and evaporites, sandstones, conglomerates; pyritised microbial mats.|
36957|Dresser Formation|70022|6|Mentioned|p113, 115|||East Pilbara Terrane.||Coongan Subgroup.||Overlies Coonterunah Subgroup.||
36957|Dresser Formation|70507|5|Briefly described|p429-433,436,442-446|Paleoarchean|Paleoarchean|Geological province: Pilbara Craton. Represents Earth's oldest proposed fossiliferous sedimentary rocks (Ueno et al., 2001; Van Kranendonk, 2011; Van Kranendonk et al., 2008; Walter et al., 1980). Exposed only in the North Pole Dome; preserved as a ring of hills surrounding the North Pole Monzogranite. U-Pb zircon dating of felsic volcaniclastic sandstones yielded max depositional age of 3.481+\-0.002 Ga (Van Kranendonk et al., 2008). Also yields c. 3490 Ma Pb-Pb galena isochron date. Lower chert-barite sections are closely associated with hydrothermal activity. Experienced repeated episodes of hydrothermal circulation within basaltic packages separated by silicified sediments acting as aquacludes, leading to horizontal variations of metamorphic overprints (Van Kranendonk, 2006). See p431-442 for carbon isotope analysis of organic matter microstructures of the Dresser Formation. Typically mature kerogen subjected to (uniform) thermal maturation.|~3.5 Ga|Unit of Warrawoona Group.||||
36957|Dresser Formation|70729|6|Mentioned|p164|||Geological province: East Pilbara Terrane, Pilbara Craton.||Unit og Talga Talga Subgroup.||||
36957|Dresser Formation|70733|6|Mentioned|p105|||Eastern Pilbara Craton.||Talga Talga Subgroup.||||
36957|Dresser Formation|70775|5|Briefly described|p12|Paleoarchean|Paleoarchean|East Pilbara.|c. 3480 Ma|Warrawoona Group||Overlies the North Star Basalt. Overlain by the Mount Ada Basalt.||
36957|Dresser Formation|70884|5|Briefly described|p123|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|c. 3.48 Ga|Unit of Talga Talga Subgroup.||Overlain by Mc Phee Formation. Underlain by North Star Basalt.||
36957|Dresser Formation|71137|6|Mentioned|p13-16|Archean|Archean|Associated with barite spring mounds and feeder dykes.|3.5 Ga.|||||
36957|Dresser Formation|71487|5|Briefly described|p128|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Talga Talga Subgroup.||||
36957|Dresser Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Warrawoona  Large Igneous Province.|max age 3481+/-3 Ma, min ~ 3477 Ma.|Talga Talga Subgroup|||Chert and mafic volcanic rock; metamorphosed.|
36957|Dresser Formation|72064|5|Briefly described|p66,82|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Hydrothermally-influenced, shallow water to terrestrial sediments, which contain potential stromatolites, geyserites and other organic carbon (Djokic et al., 2017; Glickson et al., 2008; Morag et al., 2016; Ueno et al., 2004; Van Kranendonk, 2006; Van Kranendonk et al., 2008; Walter et al., 1980).|3490 Ma|Unit of Warrawoona Group.||Overlain by McPhee Formation. Underlain by North Star Basalt.||
36957|Dresser Formation|72251|5|Briefly described|p54|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Talga Talga Subgroup.||Overlain by Mount Ada Basalt. Underlain by North Star Basalt.||
36957|Dresser Formation|72487|6|Mentioned|p10|Archean|Archean|Disagreement exists as to the origin of fusiform carbonaceous microstructures from this unit; they have been attributed to silicified vesicular volcanic glasses, not microfossils.|3.48 Ga.|||||
36957|Dresser Formation|72668|5|Briefly described|p3-5, p11, p18, p20|||East Pilbara Terrane. Features ripples and dessication cracks indicative of periods of shallow to subaerial conditions in the Warrawoona Group. Preserves the oldest evidence for life on Earth.|c. 3490 Ma|Talga Talga Subgroup.|||Includes ripples and dessication cracks in sedimentary rocks including chert-barite units.|13-JAN-22
36957|Dresser Formation|73160|4|Described|p1-7, p8 Fig.6, p9 Fig.7, p12-14|Paleoarchean|Paleoarchean|Pilbara Craton, East Pilbara Terrane. Lower part of Warrawoona Group in the North Pole Dome. Hydrothermal silica veins. U-Pb apatite age of 3214 +/- 140 Ma for a hydrothermal silica vein (Nishizawa et al., 2004), hydrothermal silica veins rarely transect the entire formation.|3481 +/- 3.6 Ma|Warrawoona Group|North Pole Chert/Lower Chert Member, Upper Chert Member.|Conformably overlies North Star Basalt, underlies Mount Ada Basalt.|Comprises two sedimentary units separated by a middle member of pillow basalt and dolerite. Hosts wrinkly, laminated, conical, and domical stromatolites in lower part. Pillow basalts are dominated by a chlorite-epidote assemblage.|
36957|Dresser Formation|73598|6|Mentioned|p1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Talga Talga Subgroup.||Overlies North Star Basalt. Is overlain by Mount Ada Basalt.||
79472|Dromedary Bore Granite|70770|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c.2945 Ma.|Bunnawarra Suite.|||Granodiorite gneiss; locally biotite-rich with K-feldspar augen.|
79472|Dromedary Bore Granite|70796|4|Described|2_5m_interpgeop15_lut.csv|Mesoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. Affected by the Yilgarn Craton granite magmatism (3010  2600 Ma); Youanmi Terrane events (3131  2600 Ma). See also 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 198213.1.pdf.|2945 +/ 6 Ma (isotopic)|Bunnawarra Suite|||Granodiorite gneiss; locally biotite rich with Kfeldspar augen|
79472|Dromedary Bore Granite|71269|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). Sample GSWA 198213 (syenogranite gneiss) yielded weighted mean 207Pb/206Pb date of 2945+\-6 Ma, interpreted as the magmatic crystallization age of the syenogranite. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|2945+\-6 Ma (isotopic)|Unit of Bunnawarra Suite.|||Granodiorite gneiss; locally biotite rich with K-feldspar augen.|
79472|Dromedary Bore Granite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Youanmi Terrane.|2945+/-6 Ma.|Bunnawarra Suite|||Granodiorite gneiss; locally biotite rich with K-feldspar augen.|
26528|Duck Creek Dolomite|22484|5|Briefly described|p79 Fig.8|||||||||
26528|Duck Creek Dolomite|22716|6|Mentioned|p234|Orosirian|Orosirian|||||||
26528|Duck Creek Dolomite|23047|6|Mentioned|35|||Of the Wyloo Group. Hamersley Province.||||||10-FEB-09
26528|Duck Creek Dolomite|23280|6|Mentioned|Table1p1085|||||||||
26528|Duck Creek Dolomite|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Wyloo Group.||||||
26528|Duck Creek Dolomite|23529|5|Briefly described|p10|||Parent: Wyloo Group.||||||28-JUL-08
26528|Duck Creek Dolomite|23575|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Wyloo Group. Overlying unit June Hill Volcanics. Underlying unit Mount McGrath Formation.||||||
26528|Duck Creek Dolomite|23589|6|Mentioned|p21|||||||||
26528|Duck Creek Dolomite|23612|5|Briefly described|p841|||||||||
26528|Duck Creek Dolomite|23774|6|Mentioned|p731|||||||||
26528|Duck Creek Dolomite|23890|4|Described|p16|Paleoproterozoic|Paleoproterozoic|Of Wyloo Group. Geological Province: Ashburton Basin. Maximum thickness: 1000m.||||||07-NOV-08
26528|Duck Creek Dolomite|24017|5|Briefly described|p13|Paleoproterozoic|Paleoproterozoic|Of the Wyloo Group.||||||07-NOV-08
26528|Duck Creek Dolomite|24544|4|Described|p47 Fig.35|Paleoproterozoic|Paleoproterozoic|Of Upper Wyloo Group. Conformably overlies Mount McGrath Formation. Conformably overlain by Ashburton Formation. Max. thickness: 1000 m. Geological Province: Ashburton Province.||||||07-NOV-08
26528|Duck Creek Dolomite|24573|5|Briefly described|p671 Fig.2|Proterozoic|Proterozoic|Of the Wyloo Group. Geological Province: Pilbara Craton.||||||28-JUL-08
26528|Duck Creek Dolomite|24602|5|Briefly described|p854 Fig. 1|||Geological Province: Ashburton Fold Belt. Of the Wyloo Group. See also p855.||||||28-JUL-08
26528|Duck Creek Dolomite|24607|4|Described|p967, 969|||Of the Wyloo Group. Conformably overlies the Mount McGrath Formation. Conformably overlain by the Ashburton Formation. Geological Province: Ashburton Basin.||||||30-NOV-10
26528|Duck Creek Dolomite|29591|6|Mentioned|p121|||||||||
26528|Duck Creek Dolomite|29716|4|Described|Table 1|||||||||
26528|Duck Creek Dolomite|29717|6|Mentioned|p1158|||||||||
26528|Duck Creek Dolomite|29848|6|Mentioned|p414|||||||||
26528|Duck Creek Dolomite|32727|6|Mentioned|p30|||||||||
26528|Duck Creek Dolomite|33543|6|Mentioned|p132|||Refers de la Hunty (1965)||||||
26528|Duck Creek Dolomite|33544|6|Mentioned|p286|||||||||
26528|Duck Creek Dolomite|33630|6|Mentioned|p908|||||||||
26528|Duck Creek Dolomite|34066|4|Described|p7|||L.Prot. See also P8.||||||
26528|Duck Creek Dolomite|34124|4|Described|Table 1|||See also PP5,6,15. Lower Proterozoic.||||||
26528|Duck Creek Dolomite|34202|6|Mentioned|p1057|||||||||
26528|Duck Creek Dolomite|34203|6|Mentioned|p13|||||||||
26528|Duck Creek Dolomite|34702|6|Mentioned|p31|||||||||
26528|Duck Creek Dolomite|34737|6|Mentioned|p355|||||||||
26528|Duck Creek Dolomite|34999|6|Mentioned|Table 17|||||||||
26528|Duck Creek Dolomite|35059|6|Mentioned|p205|||||||||
26528|Duck Creek Dolomite|35218|6|Mentioned|Fig.1|||||||||
26528|Duck Creek Dolomite|35260|5|Briefly described|p18|||||||||
26528|Duck Creek Dolomite|35269|6|Mentioned|p305|||||||||
26528|Duck Creek Dolomite|35976|6|Mentioned|Fig.38|||See also Fig.39, Table 16.||||||
26528|Duck Creek Dolomite|36551|6|Mentioned|p26|||See also Table 23.||||||
26528|Duck Creek Dolomite|36882|4|Described|p136|||||||||
26528|Duck Creek Dolomite|36891|5|Briefly described|p441|||||||||
26528|Duck Creek Dolomite|36902|6|Mentioned|p15|||||||||
26528|Duck Creek Dolomite|37327|5|Briefly described|p396|||||||||
26528|Duck Creek Dolomite|37460|3|Fully described|p121|||||||||
26528|Duck Creek Dolomite|37577|6|Mentioned|p70|||||||||
26528|Duck Creek Dolomite|38321|6|Mentioned|Table 1|||||||||
26528|Duck Creek Dolomite|38482|6|Mentioned|p15|||||||||
26528|Duck Creek Dolomite|38790|6|Mentioned|p165|||||||||
26528|Duck Creek Dolomite|38988|6|Mentioned|p6|||||||||
26528|Duck Creek Dolomite|39210|5|Briefly described|Table 1|||||||||
26528|Duck Creek Dolomite|40103|5|Briefly described|p183|||||||||
26528|Duck Creek Dolomite|40369|6|Mentioned|Plate 1|||||||||
26528|Duck Creek Dolomite|40554|5|Briefly described|p30|||||||||
26528|Duck Creek Dolomite|40905|6|Mentioned|Fig.1|||||||||
26528|Duck Creek Dolomite|40937|6|Mentioned|p28|||||||||
26528|Duck Creek Dolomite|41125|6|Mentioned|p28|||||||||
26528|Duck Creek Dolomite|41243|5|Briefly described|p257|||||||||
26528|Duck Creek Dolomite|41845|4|Described|p81|||||||||
26528|Duck Creek Dolomite|41846|4|Described|p94|||||||||
26528|Duck Creek Dolomite|41955|6|Mentioned|Fig.1 P4|||||||||
26528|Duck Creek Dolomite|41997|6|Mentioned|p78|||||||||
26528|Duck Creek Dolomite|42148|5|Briefly described|p699|||||||||
26528|Duck Creek Dolomite|42202|6|Mentioned|p512|||||||||
26528|Duck Creek Dolomite|42260|3|Fully described|p45|||||||||
26528|Duck Creek Dolomite|42277|5|Briefly described|p62|||||||||
26528|Duck Creek Dolomite|42435|6|Mentioned|Fig.1 P43|||||||||
26528|Duck Creek Dolomite|42471|4|Described|p11|||||||||
26528|Duck Creek Dolomite|42472|5|Briefly described|Map legend|||||||||
26528|Duck Creek Dolomite|42686|5|Briefly described|map legend|Proterozoic||||||||
26528|Duck Creek Dolomite|42704|5|Briefly described|Plate 2E|Proterozoic|Proterozoic|Of the Wyloo Group.||||||07-AUG-08
26528|Duck Creek Dolomite|42744|4|Described|p6|||||||||
26528|Duck Creek Dolomite|43037|5|Briefly described|Fig.2,p24|||Of Wyloo Group.||||||28-JUL-08
26528|Duck Creek Dolomite|43069|5|Briefly described|p20|||||||||
26528|Duck Creek Dolomite|43119|4|Described|p15|||Of Wyloo Group.||||||28-JUL-08
26528|Duck Creek Dolomite|43262|5|Briefly described|Map Legend||Proterozoic|Of Wyloo Group.||||||28-JUL-08
26528|Duck Creek Dolomite|43290|4|Described|p9||Proterozoic|Of Wyloo Group.||||||28-JUL-08
26528|Duck Creek Dolomite|44319|14|Not recorded|map legend||Paleoproterozoic|Wyloo Group. L.Proterozoic.||||||07-NOV-08
26528|Duck Creek Dolomite|44477|14|Not recorded|p.11, Table 1||Proterozoic|SF/50-6.||||||
26528|Duck Creek Dolomite|44478|14|Not recorded|map legend||Proterozoic|||||||
26528|Duck Creek Dolomite|44481|5|Briefly described|map legend||Proterozoic|||||||
26528|Duck Creek Dolomite|44503|14|Not recorded|p.17|||(F50-12).||||||
26528|Duck Creek Dolomite|44692|2|Defined|p.7,8,17-19,Tb.1,map|||(F50-11).||||||
26528|Duck Creek Dolomite|44729|5|Briefly described|map legend|Proterozoic||Of Wyloo Group.||||||28-JUL-08
26528|Duck Creek Dolomite|50222|5|Briefly described|p327|Paleoproterozoic|Paleoproterozoic|Of the Wyloo Group.  Age: <1.84Ga (Pidgeon and Horwitz, 1991).||||||07-NOV-08
26528|Duck Creek Dolomite|50226|5|Briefly described|p415, p416|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26528|Duck Creek Dolomite|61273|5|Briefly described|p85|Paleoproterozoic|Paleoproterozoic|Contains high-grade dolomitic marble which is quarried for dimension stone.||||||07-NOV-08
26528|Duck Creek Dolomite|61276|4|Described|p577-580|Orosirian|Orosirian|Of the Wyloo Group. Overlies the Mount McGrath Formation. Dolomite. Underlies the Ashburton Formation.||||||17-OCT-16
26528|Duck Creek Dolomite|61526|5|Briefly described|p880|||Of the Upper Wyloo Group.||||||
26528|Duck Creek Dolomite|61732|6|Mentioned|p26|Paleoproterozoic|Paleoproterozoic|Contains assemblages of microfossils.||||||07-FEB-11
26528|Duck Creek Dolomite|62129|3|Fully described|p15|Proterozoic|Proterozoic|Of Wyloo Group. Comformably underlain by Mount McGrath Formation, conformably overlian by Ashburton Formation. Thick: 1000m. Geol Prov: Ashburton Basin. Thin- to thick-bedded, buff, grey, or mauve coloured dolomite. See p15-16 for more information.||||||07-FEB-11
26528|Duck Creek Dolomite|62130|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Wyloo Group. Geological Province: Ashburton Basin. Thin- to thick-bedded, locally metamorphosed stromatolitic dolomite; metadolorudite; minor chert and pelite.||||||
26528|Duck Creek Dolomite|63432|5|Briefly described|p736 Fig. 2|Proterozoic|Proterozoic|||||||07-FEB-11
26528|Duck Creek Dolomite|63869|4|Described|p5-6, Plate 1|Paleoproterozoic|Paleoproterozoic|Thickness to 1 km. Age range from ages of surrounding units.|2209 +/- 15 Ma - 1806 Ma.|Unit in Wyloo Group.||Conformably overlies Mount McGrath Formation. Is overlain conformably by Ashburton Formation.|Thin- to thick-bedded, buff grey or mauve, laminated dolostone interlayered with thin- to very thick-bedded dolostone breccia; silicification locally intense; layers or nodules of chert; thin mudstone horizons.|
26528|Duck Creek Dolomite|64284|6|Mentioned|p59|||Of the upper Wyloo Group. Contains stromatolites.||||||07-FEB-11
26528|Duck Creek Dolomite|64384|5|Briefly described|p47 Tb. 7, p83|||Of Wyloo Group. Conformable on Mount McGrath Formation; conformably overlain by Ashburton Formation. Geological province: Ashburton Basin. Consists of thin to thick bedded grey-mauve dolomite; commonly stromatolitic.||||||07-FEB-11
26528|Duck Creek Dolomite|64772|6|Mentioned|p11|||Contains microbial assemblages. This unit is compared with Frere Formation of the Earaheedy Group.||||||07-FEB-11
26528|Duck Creek Dolomite|65830|6|Mentioned|p3|||||Of the Wyloo Group||||
26528|Duck Creek Dolomite|66115|4|Described|p135-147|Paleoproterozoic|Paleoproterozoic|Name used interchangeably with Duck Creek Formation and Duck Creek Dolomites. Defined on basis of single measured section. Thickness: >1000 m. Age: late Paleoproterozoic. Carbonate platform in Ashburton Basin. Contains distinctive microfossils. Duck Creek Dolomite micropaleontology is compared with other sites from around the world, and Frere Formation in Australia. Age max: underlying Cheela Springs Basalt 2209+/-15 Ma (SHRIMP U-Pb, Martin et al. 1998). Age min: overlying June Hill Volcanics, new U-Pb SHRIMP date on tuff reported in this paper: 1795+/-7 Ma zircon typical of magmatic growth and detrital zircon ranging from 1834-3470 Ma. Detailed mineralogy and geochemistry provided. Lithology continued: within dolomite, large-amplitude (>20cm) symmetric ripples, teepee structures, and imbricate flat-pebble conglomerates occur, along with diagenetic cherts. Third iron formation interval is in overlying Ashburton Fm. In summary, a sequence stratigraphic architecture: multiple sequences that grade upward from shallow subtidal grainstones and stromatolitic bioherms to peritidal carbonates with conspicuous precipitated microdigitate stromatolites. Maximum flooding intervals contain iron formation and other authigenic carbonate/silicate precipitates, and slope/basinal facies are marked by (dolo)micrite and limestone rhythmites, rhythmite breccias, block breccias, and carbonate turbidites. Based on the presence of turbidites and slump features distal to peri- to supratidal precipitates, the overall platform architecture is that of a distally steepened carbonate ramp.|ca. 1.8 Ga. See comments.|Wyloo Group||Conformably overlies (is graded upward from) Mount McGrath Formation. Is overlain conformably by June Hill Volcanics and Ashburton Formation.|Grades upward (from Mount McGrath Formation) into a fine-grained, white siltstone, capped by hummocky- and swaly-crosss-stratified dolomite; stromatolites; rare grainstones. Carbonates and 2 iron formation (~1m) intervals. See comments for summary.|
26528|Duck Creek Dolomite|66427|6|Mentioned|p47|||Contains stromatolites aged 1900-1800 Ma similar to taxa in Earaheedy Group.||Unit in Wyloo Group.||||
26528|Duck Creek Dolomite|66950|6|Mentioned|p4, p6|Rhyacian|Rhyacian|||Of the Wyloo Group.||||
26528|Duck Creek Dolomite|67025|5|Briefly described|p319, p320, p322 Table 3, p324.|Paleoproterozoic|Paleoproterozoic|||Unit in Wyloo Group.|||Dolomite, sandstone.|
26528|Duck Creek Dolomite|67056|5|Briefly described|p419 Fig.2. |Paleoproterozoic|Paleoproterozoic|||Unit in Upper Wyloo Group.||Overlies Mount McGrath Formation. Is overlain by June Hill Volcanics.||
26528|Duck Creek Dolomite|67130|5|Briefly described|p3 fig 2, p5, p23, p24 fig 17, p51 |||Up to 1km thick. Slope, barrier bar, lagoon, intertidal and supratidal facies.||Wyloo Group, Upper||Conformably overlies Mount McGrath Formation, conformably overlain by Ashburton Formation, gradationally interbedded with June Hill Volcanics|Stromatolitic dolomite, subtidal stromatolitic bioherms, mound and channel systems, limestones interbedded with dolomitic turbidites and iron formations and local olistostromes.|
26528|Duck Creek Dolomite|67827|5|Briefly described|p416 Fig.5, p428|Orosirian|Orosirian||~1.85 Ga-1800 Ma|Of the Upper Wyloo Group.||Overlies Mount McGrath Formation.|Stromatolitic.|
26528|Duck Creek Dolomite|67855|4|Described|p216-217, p212 fig 3-10, p214, 218|Paleoproterozoic|Paleoproterozoic|1000m thick.||Of Wyloo Group||Overlies Mount McGrath Formation (conformably), Fortescue Group, Hamersley Group (both unconformably).  Overlain by Ashburton Formation (conformably). Grades to June Hill Volcanics.|Buff or grey-mauve weathering dolomite, commonly stromatolitic.  5 major facies have been described. Lower and upper parts are thick slope deposits, but the middle 50-300m is barrier-bar/lagoon/supratidal in repeated cycles.|
26528|Duck Creek Dolomite|68035|5|Briefly described|p293, p292 fig 6|Paleoproterozoic|Paleoproterozoic|Ashburton Basin. Up to 1 km thick and consists of repeated upward-shallowing sequences formed by transgressive and regressive sedimentation on a barred carbonate shoreline (Grey and Thorne, 1985). Includes slope, barrier-bar, lagoon, intertidal and supratidal facies, together with major developments of subtidal stromatolitic bioherms.||Of upper Wyloo Group.||Conformably overlies Mount McGrath Formation. Conformably overlain by Ashburton Formation.||
26528|Duck Creek Dolomite|68280|4|Described|p5, p45, p46, p48, p50, p52, p54|Paleoproterozoic|Paleoproterozoic||~ 1800 Ma|||Overlain by Ashburton formation, overlies Mt McGrath Formation|Dolomite, shales, chert and banded iron formation with numerous stromatolites throughout. Olistostrome breccia of poorly bedded angular carbonate blocks.|16-JAN-23
26528|Duck Creek Dolomite|69003|5|Briefly described|p24-25|Paleoproterozoic|Paleoproterozoic|Ashburton Basin, Capricorn Orogen. Carbonate platform deposits.||||?Conformably overlies Mount McGrath Formation. Is ?intruded by, or interbedded with, June Hill Volcanics.||
26528|Duck Creek Dolomite|69024|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Ashburton Basin. Age constrained by the Wyloo Group.||Of the Wyloo Group.|||Thin- to thick-bedded laminated dolostone.|05-MAY-14
26528|Duck Creek Dolomite|69028|5|Briefly described|Map Legend|Orosirian|Orosirian|Ashburton and Blair Basins. Mapped with Mount McGrath Formation and Ashburton Formation as a single unit.||Of the Wyloo Group, upper.|||Wacke, mudstone, ferruginous mudstone, banded iron-formation, chert, sandstone, conglomerate, felsic and mafic volcanic rocks, and locally stromatolitic dolomite.|07-MAY-14
26528|Duck Creek Dolomite|69080|6|Mentioned|p688, p691-694, p697 Fig.11|||||Unit in Wyloo Group.||Overlies Mount McGrath Formation. Is overlain by June Hill Volcanics and Ashburton Formation.||
26528|Duck Creek Dolomite|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|||Wyloo Group|||Thin- to thick-bedded laminated dolostone|
26528|Duck Creek Dolomite|69538|6|Mentioned|p517 Fig.3, p576|Paleoproterozoic|Paleoproterozoic|W Pilbara.||Unit in Wyloo Group.||||
26528|Duck Creek Dolomite|69596|6|Mentioned|p6|||Pilbara Craton.||||||
26528|Duck Creek Dolomite|70327|6|Mentioned|p11 Fig.12, p13 Fig.16|||Duck Creek Basin.||||Overlies Mount McGrath Formation.||
26528|Duck Creek Dolomite|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_interpgeop_lut.csv|2010-1799 Ma|Wyloo Group|||Thin to very thickly bedded laminated dolostone.|
26528|Duck Creek Dolomite|70949|5|Briefly described|p988-989|Paleoproterozoic|Paleoproterozoic|Mount Olympus area. Locally hosts gold.||Wyloo Group.|||Dolomite, siltstone, chert.|
26528|Duck Creek Dolomite|70958|4|Described|p5, 4, 7, p16, Fig. 1|Paleoproterozoic|Paleoproterozoic|Thickness 1-3 km in area studied.||Of Wyloo Group||Mainly overlies, but interfingers in part with Mount McGrath Formation. Overlain by and interfingers with Mininer Turbidite Member, Ashburton Formation, on shelf edge.|Massive and bedded dolomites, stromatolitic in places. Red and black manganiferous chert and minor BIF at top in some places.|
26528|Duck Creek Dolomite|71112|5|Briefly described|p75|||Geological province: Pilbara Craton. ||||Overlain by Lower Ashburton Formation. Underlain by Mount McGrath Formation.||
26528|Duck Creek Dolomite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||crystalline dolostone/dolomite, dolorudite, chert, shale|
26528|Duck Creek Dolomite|71273|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Ashburton Basin.||Wyloo Group.|||Thin- to very thick-bedded dolostone, commonly stromatolitic or brecciated; locally silicified.|
26528|Duck Creek Dolomite|71808|6|Mentioned|p149|||||Wyloo Group, Upper||||
26528|Duck Creek Dolomite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Ashburton Basin.||Wyloo Group|||Thin- to very thick-bedded dolostone, commonly stromatolitic or brecciated; locally silicified.|
26528|Duck Creek Dolomite|72570|5|Briefly described|p2|Orosirian|Orosirian|Similarities to the Turee Creek Group reef complex led to discussions as to whether it was a faulted slice of this formation however a minimum age of 2.0 Ga for the TCG reef complex precludes this idea.|c. 1860 Ma|Wyloo Group||||
26528|Duck Creek Dolomite|72712|4|Described|p7, p9, p25, p31, p33-34.|Statherian|Statherian|Recognized by MacLeod et al. (1963). See also p52.||Wyloo Group||Conformably overlies McGrath Formation and unconformably overlies Fortescue and Hamersley Groups. Underlies June Hill Volcanics (conformity), Ashburton Formation (disconformity).|A locally silicified, stromatolitic dolomite unit.|
26528|Duck Creek Dolomite|72758|4|Described|p13 Tb.1, p31, p34-38, p40, 42, 58, 60.|Paleoproterozoic|Paleoproterozoic|Up to 1 km thick. Five major sedimentary facies are recognized: slope, barrier-bar, lagoon, intertidal, and supratidal.||Wyloo Group||Conformably overlies Mount McGrath Formation. Unconformably overlies Fortescue, Hamersley Groups. Conformably underlies Ashburton Formation, June Hill Volcanics (gradational contact).|Thin to thick bedded, locally stromatolitic dolomite with minor chert and mudstone, contains relic evaporite textures and dolomitic breccias.|
34382|Duck Creek Supersequence|22682|5|Briefly described|Fig21,p31|Orosirian|Orosirian|Age: 1997-1953 Ma. Ashburton Province.||||||03-MAR-10
74383|Duerdin Group, Lower|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Massive matrix-supported polymictic pebble to boulder conglomerate; larger clasts striated; poorly sorted lithic sandstone and dolomitic sandstone, pebble to cobble sandstone; minor thin-bedded dolomite|
36127|Duluth Complex|23455|6|Mentioned|p44|||||||||
36887|Dumbie Granodiorite|23485|4|Described|p22|Paleoproterozoic|Paleoproterozoic|Of Moorarie Supersuite.||||||07-NOV-08
36887|Dumbie Granodiorite|23486|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Moorarie Supesuite. Geological Province: Gascoyne Complex.||||||07-NOV-08
36887|Dumbie Granodiorite|23525|4|Described|p22|Orosirian|Orosirian|Intrudes the Halfway Gneiss.   Age: 1810+/-9Ma, 1811+/-6Ma (SHRIMP U/Pb). Geological Province: Gascoyne Complex||||||25-JAN-08
36887|Dumbie Granodiorite|23527|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Moorarie Supersuite, Gascoyne Complex||||||07-NOV-08
36887|Dumbie Granodiorite|23780|5|Briefly described|p28|Paleoproterozoic|Paleoproterozoic|Age: ~1800+/-7 Ma||||||07-NOV-08
36887|Dumbie Granodiorite|23781|5|Briefly described|p58|Paleoproterozoic|Paleoproterozoic|Of Moorarie Supersuite.  Age: c.1810Ma.||||||07-NOV-08
36887|Dumbie Granodiorite|24544|4|Described|p10 Tb.1|Paleoproterozoic|Paleoproterozoic|Age: c. 1810 Ma. Of Moorarie Supersuite. Intrudes Halfway Gneiss.||||||07-NOV-08
36887|Dumbie Granodiorite|50218|5|Briefly described|p240 Fig.2|Paleoproterozoic|Paleoproterozoic|Of the Moorarie Supersuite. Age: c.1810Ma. Geological Province: Gascoyne Complex.||||||07-FEB-11
36887|Dumbie Granodiorite|50219|5|Briefly described|p260 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Moorarie Supersuite.  Age: c.1810Ma.  Geological Province: Gascoyne Complex.||||||07-FEB-11
36887|Dumbie Granodiorite|63866|5|Briefly described|p157|Orosirian|Orosirian|Glenburgh Terrane. SHRIMP ages derived from Occhipinti and Sheppard, 2001.|1811 +/- 6 Ma and 1810 +/- 9 Ma (U-Pb SHRIMP)|Moorarie Supersuite|||Granite and pegmatite.|
36887|Dumbie Granodiorite|66110|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Moorarie Supersuite. Porphyritic, fine- to medium-grained granodiorite; minor monzogranite; medium to coarse tabular phenocrysts of K-feldspar; locally magnetite and allanite bearing.||||||
36887|Dumbie Granodiorite|66299|4|Described|p10, pp146-147, p210.|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, Gascoyne Province. LREE-enriched granites. Parts were syn-tectonic with D1 of Capricorn Orogeny.|1811 +/- 9 Ma to 1804 +/- 5 Ma.|Unit in Moorarie Supersuite.||Cross-cut by plutons and dykes of Scrubber Granite. Intrudes Halfway Gneiss. Is unconformably overlain by Edmund Group.|Porphyritic, fine- to medium-grained granodiorite; minor monzogranite; medium to coarse tabular phenocrysts of K-feldspar; locally magnetite and allanite bearing.|
36887|Dumbie Granodiorite|66579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Unit in Moorarie Supersuite.|||Porphyritic, fine- to medium-grained granodiorite; minor monzogranite; medium to coarse tabular phenocrysts of K-feldspar; locally magnetite and allanite bearing.|
36887|Dumbie Granodiorite|66950|6|Mentioned|p21|||||||||
36887|Dumbie Granodiorite|67247|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|1817 - 1776 Ma.|Unit in Moorarie Supersuite.|||Porphyritic, fine- to medium-grained granodiorite; minor monzogranite; medium to coarse tabular phenocrysts of K-feldspar; locally magnetite and allanite bearing.|
36887|Dumbie Granodiorite|67371|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.||Unit in Moorarie Supersuite.|||Porphyritic, fine- to medium-grained granodiorite; minor monzogranite; medium to coarse tabular phenocrysts of K-feldspar; locally magnetite and allanite bearing.|
36887|Dumbie Granodiorite|67373|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|1811 - 1799 Ma.|Unit in Moorarie Supersuite.|||Porphyritic, fine- to medium-grained granodiorite; minor monzogranite; medium to coarse tabular phenocrysts of K-feldspar; locally magnetite and allanite bearing.|
36887|Dumbie Granodiorite|67843|5|Briefly described|p13.|Paleoproterozoic|Paleoproterozoic|Mooloo Zone.|c.1810 Ma.|||||
36887|Dumbie Granodiorite|68521|5|Briefly described|Map Legend|Statherian|Orosirian|Geochronology by Evans et al. (2003).|c.1830-1780 Ma|Of the Moorarie Supersuite.|||Porphyritic, fine- to medium-grained granodiorite; minor monzogranite; medium to coarse tabular phenocrysts of K-feldspar; locally magnetite and allanite bearing.|
36887|Dumbie Granodiorite|68522|5|Briefly described|Map Legend|Statherian|Orosirian|Gascoyne Province. |1820-1775 Ma|Of the Moorarie Supersuite.|||Porphyritic, fine- to medium-grained granodiorite; minor monzogranite; medium to coarse tabular phenocrysts of K-feldspar; locally magnetite and allanite bearing.|
36887|Dumbie Granodiorite|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|||Moorarie Supersuite|||Porphyritic, fine- to medium-grained granodiorite; minor monzogranite; medium to coarse tabular phenocrysts of K-feldspar; locally magnetite and allanite bearing|
36887|Dumbie Granodiorite|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv|1817-1776 Ma|||Intruded by Scrubber Granite|Porphyritic, fine- to medium-grained granodiorite; minor monzogranite; medium to coarse tabular phenocrysts of K-feldspar; locally magnetite and allanite bearing.|
36887|Dumbie Granodiorite|70814|6|Mentioned|p63|||||||||
36887|Dumbie Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite, tonalite|
36887|Dumbie Granodiorite|71869|5|Briefly described|p6, app p6|||Capricorn Orogen.|1810 +/- 9 Ma, 1804+/- 5 Ma (cryst.)|Moorarie Supersuite|||Foliated porphyritic biotite granodiorite and metatonalite.|
73989|Dumont complex|63712|6|Mentioned|p825|||Identified by Duke (1986a).||||||22-NOV-07
23565|Dunnsville Granodiorite|41786|4|Described|p331|||||||||
23565|Dunnsville Granodiorite|42740|5|Briefly described|map legend|Archean||||||||07-NOV-08
23565|Dunnsville Granodiorite|43102|5|Briefly described|Fig.4|||||||||
23565|Dunnsville Granodiorite|43125|4|Described|p8, and map insert|Archean|Archean|||||||03-MAR-10
23565|Dunnsville Granodiorite|43232|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
23565|Dunnsville Granodiorite|60076|5|Briefly described|p45 App. 1|||[Aggdn]   Medium- to coarse-grained granodiorite.||||||
23565|Dunnsville Granodiorite|65204|6|Mentioned|p17 Tbl.2.|Neoarchean||0.5-6mm grains; seriate to porphyritic ||||||
23565|Dunnsville Granodiorite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Medium- to coarse-grained granodiorite; penetrative foliation and subhorizontal mineral lineation; sheared contacts with greenstones.||||||07-FEB-11
23565|Dunnsville Granodiorite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Medium- to coarse-grained granodiorite; penetrative foliation and subhorizontal mineral lineation; sheared contacts with greenstones have subhorizontal to steep mineral lineation.|05-AUG-15
23565|Dunnsville Granodiorite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Medium- to coarse-grained granodiorite; penetrative foliation and subhorizontal mineral lineation; sheared contacts with greenstones have subhorizontal to steep mineral lineation.|
23565|Dunnsville Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite|
23565|Dunnsville Granodiorite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 100k_geologyp10_lut.csv.|3010-2600 Ma (inferred)||||Medium- to coarse-grained granodiorite; penetrative foliation and subhorizontal mineral lineation; sheared contacts with greenstones have subhorizontal to steep mineral lineation|
25888|Dupuy Formation|12466|6|Mentioned|p175.|||Hydrocarbons evident, but no oil produced on test.||||||
25888|Dupuy Formation|12491|6|Mentioned|p453, p460-462, p464-466.|Early Cretaceous|Late Jurassic|Syn-rift deposition filling in sub-basin and half-grabens on Exmouth Plateau.||||Overlies Dingo Claystone. Is overlain by Barrow Group.||06-NOV-14
25888|Dupuy Formation|23379|4|Described|p160 Fig.2;p158,159,162,164,165,167,169|Berriasian|Kimmeridgian|Of Barrow Sub-basin, Carnarvon Basin.||||||01-SEP-08
25888|Dupuy Formation|23726|5|Briefly described|p8 Fig 2c|Jurassic|Jurassic|Underlying unit Biggada Formation. Geological Province: Carnarvon Basin.||||||
25888|Dupuy Formation|24084|5|Briefly described|p146 Fig.2|Late Jurassic|Late Jurassic|Geological Province: North Carnarvon Basin.||||||16-MAR-05
25888|Dupuy Formation|24331|5|Briefly described|p475 Fig.2|Early Cretaceous|Late Jurassic|Conformably overlies Dingo Claystone. Overlain by Malouet Formation and Barrow Group (conformable). Marine. Geological Province: Barrow Sub-basin.||||||21-DEC-04
25888|Dupuy Formation|24351|5|Briefly described|Plate 4 (in pocket)|Late Jurassic|Late Jurassic|Geological Province: Exmouth Sub-basin.||||||13-DEC-07
25888|Dupuy Formation|24390|5|Briefly described|p24 Table 6|||Geological Province: Northern Carnarvon Basin.||||||
25888|Dupuy Formation|37306|6|Mentioned|p42|||||||||
25888|Dupuy Formation|40617|2|Defined|p8|Middle Jurassic|Early Jurassic|Early to Middle Jurassic.||||||08-OCT-15
25888|Dupuy Formation|41271|3|Fully described|p127|||||||||
25888|Dupuy Formation|41436|6|Mentioned|p47|||||||||
25888|Dupuy Formation|41438|6|Mentioned|p106|||||||||
25888|Dupuy Formation|41440|4|Described|p137|||||||||
25888|Dupuy Formation|41446|6|Mentioned|Fig.2|||||||||
25888|Dupuy Formation|41732|6|Mentioned|p534|||||||||
25888|Dupuy Formation|42116|5|Briefly described|Fig.1 P6|||||||||
25888|Dupuy Formation|42598|5|Briefly described|p90|||||||||
25888|Dupuy Formation|42615|3|Fully described|p36|||Age early Kimmeridgian to latest Tithonian.||||||01-SEP-08
25888|Dupuy Formation|43712|6|Mentioned|p11|||||||||
25888|Dupuy Formation|43722|6|Mentioned|p10|||||||||
25888|Dupuy Formation|43724|6|Mentioned|p29|||||||||
25888|Dupuy Formation|43826|6|Mentioned|Fig.2,p163||Late Jurassic|||||||01-MAR-10
25888|Dupuy Formation|50085|6|Mentioned|p24 Tb. 6|||Geological Province: Northern Carnarvon Basin.||||||
25888|Dupuy Formation|60116|6|Mentioned|p23|||Possibly to be used for carbon dioxide sequestration.||||||22-JUL-04
25888|Dupuy Formation|60386|6|Mentioned|p302|Berriasian|Late Jurassic|Northern Carnarvon Basin. Proximal shelf.||||||
25888|Dupuy Formation|61555|5|Briefly described|p236, 239|Tithonian|Tithonian|Exmouth Sub-basin. Overlies Dingo Claystone. Unconformably overlain by Macedon Member. Marine silty claystone.||||||
25888|Dupuy Formation|62734|5|Briefly described|p1362 Fig. 2|Late Jurassic|Late Jurassic|Geological Province: Barrow Sub-basin.||||||01-SEP-08
25888|Dupuy Formation|62837|5|Briefly described|Stratigraphic columns|Middle Jurassic|Middle Jurassic|Age: >145Ma. Geological Province: Exmouth Sub-basin and Barrow Sub-basin.||||||01-MAR-10
25888|Dupuy Formation|63950|5|Briefly described|p336 Fig. 4, p338|Tithonian|Kimmeridgian|Geological Province: northern Carnarvon Basin. A submarine fan complex forming a thick succession of deep marine claystones has infilled much of the Dampier Sub-basin.||||||27-MAY-08
25888|Dupuy Formation|64977|6|Mentioned|p493 Fig.3.|Early Cretaceous|Late Jurassic|Thevenard Island area.||||Overlies Dingo Claystone. Is overlain by Barrow Group.||
25888|Dupuy Formation|66126|6|Mentioned|p206|Late Jurassic|Late Jurassic|Carnarvon Basin.||||||
25888|Dupuy Formation|67200|5|Briefly described|p8 fig 6, p54, p64, p65|Jurassic|Jurassic|Thermal conductivity of 2.29 W/mK||||Overlies Biggada Formation|Sandstone and Siltstone.|
25888|Dupuy Formation|68135|5|Briefly described|p51 fig 2a|Early Cretaceous|Late Jurassic|Northern Carnarvon Basin.||||Is overlain unconformably by Barrow Group.||14-SEP-17
25888|Dupuy Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Northern Carnarvon Basin.||||||
25888|Dupuy Formation|70066|5|Briefly described|Regional: Fig.6; p6, p16|Tithonian|Kimmeridgian|Exmouth and Barrow Sub-basins, Northern Carnarvon Basin. Significant petroleum reservoir.|||Eskdale Member.|Overlies Dingo Claystone. Is overlain by Barrow Group.||
37648|Durlacher Supersuite|24544|4|Described|p42|Statherian|Statherian|Age: 1680-1620 Ma.||||||
37648|Durlacher Supersuite|61262|2|Defined|p458 App., p448-450, p447 Fig. 4.|Paleoproterozoic|Paleoproterozoic|Pimbyana, Dingo Creek and Yangibana Granites and several unnamed units. Plutons, plugs and dykes; monzogranite, granodiorite, lesser syenogranite, tonalite and gabbro; intrude Poorananoo Metamorphics. Unconformably underlies Edmund Gp. Age: 1680-1620Ma.||||||07-NOV-08
37648|Durlacher Supersuite|63246|5|Briefly described|p478 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 1680-1620Ma. In the Gascoyne Complex. Three composite plutons comprising foliated granites (intruded Morrissey and Pooranoo Metamorphics) and massive biotite-muscovite-tourmaline granite.||||||07-NOV-08
37648|Durlacher Supersuite|63469|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Includes Davey Well Granite. Consists of granodiorite, monzogranite, metamonzogranite, metagranodiorite, metasyenogranite, metamorphosed dolerite and leucogabbro, qtz gabbro, schist and metamorphosed ultramafic rock.||||||07-NOV-08
37648|Durlacher Supersuite|63470|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes Dingo Creek, Pimbyana and Yangobana Granites. Geological Province: Gascoyne Complex. Comprises granodiorite, augen gneiss, monzogranites, metamonzogranite to metasyenogranite, and syenogranite.||||||07-NOV-08
37648|Durlacher Supersuite|63471|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes Pinbyana (probably misspelt? placename is Pimbyana) and Dingo Creek Granites. Age: 1680-1620Ma. Geological Province: Gascoyne Complex.||||||07-NOV-08
37648|Durlacher Supersuite|63866|5|Briefly described|p152, p160, p162, p177|||Emplaced during the Mangaroon Orogeny.|c. 1680-1620 Ma||Includes the Dingo Creek Granite, Pimbyana Granite and Yangibana Granite.||Granitic and minor gabbroic intrusions.|
37648|Durlacher Supersuite|63869|4|Described|p1, p4, p5, p10, p18, p20, p22, p25-27|Paleoproterozoic|Paleoproterozoic|See also p46, p52, p57, Plate 1. Newly defined unit. Associated with peak metamorphism of the Mangaroon Orogeny. Intrusions continued to c.1620 Ma.|1680-1660 Ma.||Includes Yangibana, Dingo Creek and Pimbyana Granites.|Intrudes Gascoyne Complex and Yarlarweelor Gneiss Complex.|Granite, monzogranite, tonalite, granodiorite; minor gabbro.|
37648|Durlacher Supersuite|64580|4|Described|map legend||Paleoproterozoic|Radiogenic granite; Minor metagabbro with xenocrysts of quartz and K-feldspar; massive. Foliated and gneissic granite. Three descriptions give age as Paleoproterozoic, the other says Devonian.||||||
37648|Durlacher Supersuite|64728|6|Mentioned|p97, p106, p109 Fig.11.|||Unmetamorphosed granites intruding the Gascoyne Complex.|1680-1620 Ma.||||Granites.|
37648|Durlacher Supersuite|65152|5|Briefly described|p3.|Paleoproterozoic|Paleoproterozoic|Gascoyne Complex. Voluminous granite intrusions between 1680 and 1620 Ma.||||||01-MAY-15
37648|Durlacher Supersuite|65450|5|Briefly described|p1, p2 Fig.1, p7|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Pb mineralisation.|1680-1660/1620 Ma.|||Granite plutons intrude Pooranoo Metamorphics at 1680-1660 Ma.|Granite.|
37648|Durlacher Supersuite|65453|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Intrudes Leake Spring Metamorphics and Moorarie Supersuite. Age: 1680-1620 Ma (geochronology: Sheppard et al, 2005). Geol. Prov: Gascoyne Province.||||||
37648|Durlacher Supersuite|65549|5|Briefly described|Map Legend|Statherian|Statherian|Of the Gascoyne Province. Includes Discretion Granite. Shown as older than Edmund Group, Bangemall Supergroup. Age of c. 1620 Ma given.||||||
37648|Durlacher Supersuite|65830|3|Fully described|p20, p22, p26-34; Plates 1,2|Statherian|Statherian|Of the Mangaroon Zone.|1680-1620 Ma|Of the Gascoyne Complex.|Includes Pimbyana and Dingo Creek Granites.|Intrudes the Pooranoo Metamorphics, Gascoyne Complex, Yarlarweelor Gneiss Complex.|Comprises biotite-muscovite monzogranite, granodiorite, and syenogranite, with subordinate leucocratic muscovite-tourmaline(-biotite) granite and biotite granodiorite.|
37648|Durlacher Supersuite|66105|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Age: 1677-1619 Ma (geochronology: Sheppard et al, 2005). Leucocratic monzogranite; tourmaline-muscovite pegmatite and coarse-grained granite; leucocratic tourmaline-muscovite monzogranite. ||||||
37648|Durlacher Supersuite|66110|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Age shown as 1677-1619 Ma. Includes Pimbyana and Dingo Creek Granites as well as several unnamed units of granite, monzogranite, pegmatite, metamonzogranites and metagabbro.||||||
37648|Durlacher Supersuite|66112|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Aged c.1620 Ma. Shown as consisting only of Discretion Granite.||||||
37648|Durlacher Supersuite|66299|4|Described|p4 Fig.2, pp238-239, pp247-290. |Paleoproterozoic|Paleoproterozoic|Gascoyne Province. These granites have xenocryst ages consistent with an origin by melting of siliciclastic metasedimentary rocks of Pooranoo Metamorphics. Most are strongly peraluminous with S-type characters. Inclusions include Gooche Gneiss.|1696 +/- 20 Ma to 1619 +/- 15 Ma.||Includes Pimbyana, Dingo Creek, Davey Well and Yangibana Granites.|Veins, dykes and plutons intrude units of Pooranoo Metamorphics. Intrudes Moorarie Supersuite units and Morrissey Metamorphics. In faulted contact with or overlain by Yilgatherra Formation.|Granite and minor gabbro and metamorphosed equivalents; locally strongly foliated.|
37648|Durlacher Supersuite|66579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||1677-1604 Ma.||||Leucocratic, medium-grained, muscovite-biotite granodiorite and monzogranite; equigranular to weakly porphyritic.|
37648|Durlacher Supersuite|66887|5|Briefly described|p3 Fig.2, p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Southern Gascoyne Province.|~1675-~1620 Ma estimated from Fig.4.|||||
37648|Durlacher Supersuite|66950|5|Briefly described|p3 Fig.2, p9 Fig.8, p10 Fig.9, p12, p13|Statherian|Statherian|Gascoyne Province.|c. 1680-1620 Ma||Includes the Discretion Granite.|Intrudes the Yarlarweelor Gneiss Complex.||
37648|Durlacher Supersuite|67346|6|Mentioned|p794 Fig.1|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.||||||11-MAY-12
37648|Durlacher Supersuite|67373|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Mapped as 7 separate units, only two of which are named.|1667 - 1619 Ma.||Includes Tetlow and Davey Well Granites.||Metamonzogranites; meta-quartz diorite and tonalite; metasyenogranite; seriate to coarsely porphyritic mesocratic gneiss; sheets and dykes of metagranodiorite to metamonzogranite with inclusions of amphibolite, calc-silicate, and older granites.|
37648|Durlacher Supersuite|67843|5|Briefly described|p2 Fig.1, p5. |Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Intrusions associated with the 1680-1620 Ma Mangaroon Orogeny.||||||
37648|Durlacher Supersuite|67888|6|Mentioned|p52, p53||||||||Gneissic granites.|
37648|Durlacher Supersuite|68521|5|Briefly described|Map Legend|Statherian|Statherian|12 facies, of which 3 are named, are mapped separately. Geochronology from Sheppard et al. (2005).|c.1680-1620 Ma||Includes Dingo Creek Granite, Davey Well Granite, and Tetlow Granite.|||
37648|Durlacher Supersuite|68522|5|Briefly described|Map Legend|Statherian|Statherian|Gascoyne Province. 13 sub-units, 3 of which are named, are mapped separately. Geochronology from Sheppard et al.(2005).|1680-1620 Ma||Includes Dingo Creek Granite, Davey Well Granite, and Tetlow Granite.|||
37648|Durlacher Supersuite|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic||||||granite and minor gabbro|
37648|Durlacher Supersuite|69003|5|Briefly described|p4, p9 Fig.9, p33-35, p43|||Capricorn Orogen. Associated with the Mangaroon Orogeny.|1680-1620 Ma.|||Is overlain nonconformably by Edmund Group. Intrudes Pooranoo Metamorphics. Intruded by Gifford Creek Carbonatite Suite.||
37648|Durlacher Supersuite|69011|5|Briefly described|Map Legend|Statherian|Statherian|Gascoyne Province. Also includes 7 unnamed and separately-mapped sub-units.|1680-1620 Ma||Includes the Davey Well Granite.||Includes metamonzogranite, metagranodiorite, metasyenogranite, monzogranite, and granodiorite.|24-APR-14
37648|Durlacher Supersuite|69028|5|Briefly described|Map Legend|Statherian|Statherian|Gascoyne Province.|||||Includes granite and minor gabbro, and metamorphosed equivalents.|
37648|Durlacher Supersuite|69080|5|Briefly described|p684, p689, p690, p694 Fig.9, p696-697|Statherian|Statherian|Gascoyne Province. Associated with the 1680-1620 Ma Mangaroon Orogeny.|1680-1620 Ma.||||Granite and minor gabbro and metamorphosed equivalents.|
37648|Durlacher Supersuite|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Age derived from samples of monzogranite (169092.1.pdf, 88412.1.pdf)|1681  +/-10 Ma, 1801  +/- 5 Ma  (SHRIMP)|Gascoyne Complex|Includes Davey Well Granite, Dingo Creek Granite, Discretion Granite, Pimbyana Granite, Yangibana Granite, Tetlow Granite||Biotite granodiorite, flow banded monzogranite. Biotite granite, biotite monzogranite, muscovite-biotite granodiorite, tourmaline-muscovite pegmatite, tourmaline-muscovite monzogranite, biotite metamonzogranite, metasyenogranie, gneiss.|
37648|Durlacher Supersuite|69185|4|Described|500k_geologyp08_lut.csv||Paleoproterozoic|Geological Province: Pilbara Craton.|||||Granite and minor gabbro, metagabbro with xenocrysts of quartz and K-feldspar; massive|
37648|Durlacher Supersuite|69237|5|Briefly described|p1, p3|Statherian|Statherian|Gascoyne Province. Hosts the numerous ironstone (magnetite, haematite and goethite) veins and pods surrounded by zones of dfenitisation, of the Gifford Creek Ferrocarbonatite Complex.|1680-1620 Ma.||Pimbyana, Yangibana Granites.|||
37648|Durlacher Supersuite|69387|4|Described|p3, p9, p11-12, p15-25, p27-35, p37, p50|Statherian|Statherian|Gascoyne Province. Deformations discussed; structural fabric diagrams. SG and magnetic susceptibility values given. Gravity and magnetic modelling. Consists largely of large batholiths, ~5 to 10km thick, with tabular geometries. Hosts Pb mineralisation.|1680-1620 Ma.|||Intrudes Yarlarweelor Gneiss Complex and Moorarie Supersuite. Is intruded by Thirty Three Supersuite.|Granitic intrusions.|
37648|Durlacher Supersuite|69546|5|Briefly described|p100-102,105,107|Statherian|Statherian|Geological province: Gascoyne Province. Intruded by Gifford Creek Ferrocarbonite Complex.|1680-1620 Ma||Includes Pimbyana Granite and Yangabina Granite.|||
37648|Durlacher Supersuite|69583|5|Briefly described|Plate 3|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|1683-1619 Ma.||||Granite and minor gabbro, and metamorphosed equivalents.|
37648|Durlacher Supersuite|69596|5|Briefly described|p5-6, p9, p12|Statherian|Statherian|Gascoyne Province.|1680-1620 Ma.|||Intrudes Pooranoo Metamorphics.|Voluminous granitic rocks.|
37648|Durlacher Supersuite|70019|5|Briefly described|p93-94|Statherian|Statherian|Geological province: Gascoyne Province, Capricorn Orogen. |1680-1620 Ma|||||
37648|Durlacher Supersuite|70127|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Also includes seven facies and facies associations which are mapped separately.|1682-1619 Ma.||Pimbyana, Dingo Creek and Davey Well Granites.||Granite, monzogranite, granodiorite, syenogranite, metagabbro and metamonzogranite.|09-NOV-15
37648|Durlacher Supersuite|70138|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Coeval with Mangaroon Orogeny. Eight un-named sub-units are mapped separately.|1682-1619 Ma.||Pimbyana, Dingo Creek and Davey Well Granites.|||09-NOV-15
37648|Durlacher Supersuite|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 2_5m_interpgeop15_lut.csv, 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 169092.1.pdf West Australian Craton|1683-1619 Ma||Includes Davey Well Granite|Intrudes Spring Camp Formation|Equigranular metamonzogranite, foliated muscovite metamonzogranite, metagranodiorite, gneissic-schistose biotite metamonzogranite and metasyenogranite. Gneiss, metagabbro, metaultramafic rock, granite and minor gabbro.|
37648|Durlacher Supersuite|70814|5|Briefly described|p3-p4, p35, p49, p67|Statherian|Statherian||1680-1620 Ma||Includes the Dingo Creek, Pimbyana, Yangibana and Discretion Granites.|||
37648|Durlacher Supersuite|70826|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|Intruded during the Mangaroon Orogeny. |1682-1619 (age of orogeny)|||||
37648|Durlacher Supersuite|71000|6|Mentioned|p65|Paleoproterozoic|Paleoproterozoic|Southern Gascoyne Province.||||||
37648|Durlacher Supersuite|71169|5|Briefly described|p76|Statherian|Statherian|Emplaced during the Mangaroon Orogeny.|1680-1620 Ma ||||Granites.|
37648|Durlacher Supersuite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, granodiorite, tonalite, syenite|
37648|Durlacher Supersuite|71273|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Four facies are mapped separately.|1682-1619 Ma.||||Medium-grained monzogranites: locally garnet-bearing, equigranular to weakly porphyritic, or porphyritic with small biotite-rich clots. Granodiorite and flow-banded monzogranite, both with abundant inclusions.|16-FEB-18
37648|Durlacher Supersuite|71484|6|Mentioned|p125|||Geological province: Of Edmund and Collier basins [?].|||||Granite.|30-AUG-19
37648|Durlacher Supersuite|71804|6|Mentioned|p403 fig 10|||Gascoyne Province.||||||
37648|Durlacher Supersuite|71869|5|Briefly described|p3-p4, p7, p10-p13, p16-p18, app p13|||Gascoyne Province. Emplaced during the Mangaroon Orogeny. Oxygen analyses are discussed.|1680-1620 Ma||Includes the Discretion Granite, Davey Well Granite, Tetlow Granite, Yangibana Granite, Pimbyana Granite and Dingo Creek Granite.||Monzogranites, granodiorites and syenogranites.|
37648|Durlacher Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Capricorn Orogen.|max age 1682+/-4 Ma, min 1619+/-15 Ma.||||Granite and minor gabbro, and metamorphosed equivalents. Massive metagabbro with xenocrysts of quartz and K-feldspar.|
37648|Durlacher Supersuite|72259|6|Mentioned|p3, App. Tb.B|Statherian|Statherian||ca. 1680-1620 Ma||||Includes porphyritic biotite monzogranite, biotite-garnet schist, leucocratic muscovite-biotite monzogranite, and porphyritic muscovite-biotite monzogranite.|
37648|Durlacher Supersuite|72705|5|Briefly described|p4, 14, 16|||Gascoyne Province. Voluminous felsic magmatism associated with the Mangaroon Orogeny.|1680 - 1620 Ma.|||Is overlain unconformably by Edmund Group.|Granites.|
37648|Durlacher Supersuite|73102|5|Briefly described|p3, p8, p20|Statherian|Statherian|Gascoyne Province.|1689-1619 Ma|||Intruded by Minga Dolerite and Kulkatharra Dolerite.|Granite and minor gabbro and metamorphosed equivalents.|
37648|Durlacher Supersuite|73168|6|Mentioned|p758|||Gascoyne Province.||||||
37648|Durlacher Supersuite|73214|5|Briefly described|p974 Fig.1|Palaeoproterozoic|Palaeoproterozoic|Affected by the 1680-1629 Ma Mangaroon Orogeny.||||||
37648|Durlacher Supersuite|73442|5|Briefly described|p3|||Gascoyne Province.|||||Granite and minor gabbro and metamorphosed equivalents.|
37648|Durlacher Supersuite|74493|5|Briefly described|p2|Statherian|Statherian|Gascoyne Province, Mangaroon Zone.|c. 1680-1620 Ma|||Unconformably underlies Edmund Group|Granitic rocks.|
37648|Durlacher Supersuite|74494|5|Briefly described|p1008|Mesoproterozoic|Mesoproterozoic||||Pimbyana Granite, Yangibana Granite|Intruded by Gifford Creek Carbonatite Complex|Granitoids.|
73691|Dwarf Well Granite|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Of Carrington Suite. Coarse-grained biotite granite, metamorphosed.||||||15-DEC-08
73691|Dwarf Well Granite|68994|4|Described|p4, p6-9, p11, p13, p20, p23-p24, p26-27|Statherian|Statherian|Aileron Province. Magmatic crystallisation age; 2488-1841 Ma inherited zircons (Kirkland et al. 2009) have Hf analyses provided in this paper.|1773+/-6 Ma (U-Pb; zircon).|Carrington Suite||Is overlain by Lake Mackay Quartzite.|Unit sampled is coarse grained, strongly foliated metagranodiorite transected by local shear zones.|13-JAN-17
73691|Dwarf Well Granite|69031|5|Briefly described|p6-7|Statherian|Statherian|West Arunta Orogen.|1773 +/- 6 Ma (Kirkland et al., 2009).|Carrington Suite.||Is overlain nonconformably by Lake Mackay Quartzite.||
73691|Dwarf Well Granite|70762|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Orogen, North Australian Craton.|c.1773 Ma.|Carrington Suite.|||Coarse-grained biotite metamonzogranite.|
73691|Dwarf Well Granite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Orogen.|Max age 1773+/-6 Ma.|Carrington Suite|||Coarse-grained biotite metamonzogranite.|
23567|Eagle Hawk Sandstone|13194|6|Mentioned|p395 Tb. 4-16|||Of Ord Basin.||||||
23567|Eagle Hawk Sandstone|14019|3|Fully described|p24|Middle Cambrian|Middle Cambrian|Of the Elder Subgroup. Comprises fine to medium sandstone, minor siltstone and mudstone. Conformably overlies the Panton Formation; conformably under the Overland Sandstone. Max. thickness type section: 210m. Geol. Prov: Ord Basin.||||||10-MAY-05
23567|Eagle Hawk Sandstone|40993|6|Mentioned|Fig.1|||||||||
23567|Eagle Hawk Sandstone|41840|2|Defined|p43||Middle Cambrian|New name. Replaces Hudson Formation of Sweet 1974.||||||
23567|Eagle Hawk Sandstone|41864|3|Fully described|p24|||Unit called Hudson Formation where it crops out in NT.||||||15-DEC-08
23567|Eagle Hawk Sandstone|41865|5|Briefly described|Map legend||Middle Cambrian|||||||
23567|Eagle Hawk Sandstone|41866|5|Briefly described|Map legend|Late Cambrian||||||||
23567|Eagle Hawk Sandstone|43855|5|Briefly described|Map Legend|Boomerangian|Templetonian|||||||
23567|Eagle Hawk Sandstone|44230|5|Briefly described|Map Legend||Middle Cambrian|||||||
23567|Eagle Hawk Sandstone|44868|5|Briefly described|Map Legend|Boomerangian|Ordian|||||||
23567|Eagle Hawk Sandstone|60419|4|Described|p1, 11|Middle Cambrian|Middle Cambrian|Of Elder Subgroup. Conformably overlies Panton Formation. Overlain by Overland Sandstone. Thickness: 210 m. Intertidal. Contains ichnofossils. Geological Province: Ord Basin.||||||
23567|Eagle Hawk Sandstone|60519|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Elder Subgroup (Goose Hole Group). Fine grained, micaceous, feldspathic snadstone; minor siltstone. Geological Province: Ord Basin.||||||05-NOV-04
23567|Eagle Hawk Sandstone|60589|5|Briefly described|Map legend|Late Cambrian|Middle Cambrian|Of the Elder Subgroup.  Fine to medium micaceous and feldspathic sandstone; minor siltstone and mudstone.   Conformably overlies Panton Formation; conformably overlain by the Overland Sandstone.  Geological Province: Ord Basin.||||||24-NOV-04
23567|Eagle Hawk Sandstone|64580|6|Mentioned|map legend|||Of Goose Hole Group.||||||15-DEC-08
23567|Eagle Hawk Sandstone|67860|4|Described|p417,421,422 Figs.4.85-87; p419 Tb.4-18|Late Cambrian|Middle Cambrian|75-210 m thick. Type section details given. Contains trilobite trails.||Elder Subgroup||Conformably overlies Panton Formation. Is overlain conformably by Overland Sandstone. Equivalent to Hart Spring Sandstone (Bonaparte Basin).|Red micaceous feldspathic sandstone; minor siltstone.|
23567|Eagle Hawk Sandstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Furongian|Furongian|Ord Basin||Elder Subgroup|||Red micaceous feldspathic sandstone; minor siltstone|31-JUL-15
23567|Eagle Hawk Sandstone|69165|5|Briefly described|100k_interpgeop_lut.csv|Furongian|Furongian|See also 500k_geologyp08_lut.csv. ||Elder Subgroup|||Red Micaceous feldspathic sandstone; minor siltstone.|
23567|Eagle Hawk Sandstone|69437|5|Briefly described|p22:10-11|Series 3|Series 3|Ord Basin, Centralian B Superbasin. Sequence 2. Peritidal deposits.||||Overlies Panton Formation. Is overlain by Overland Sandstone.||12-JUL-16
23567|Eagle Hawk Sandstone|69446|6|Mentioned|p31:4|||Ord Basin.||||||12-JUL-16
23567|Eagle Hawk Sandstone|69447|6|Mentioned|p32:2|||Ord Basin.||||Broadly correlated with Point Wakefield beds (Wiso Basin).||12-JUL-16
23567|Eagle Hawk Sandstone|69448|3|Fully described|p33:2-4, 6-8|Middle Cambrian|Middle Cambrian|Mory and Beere (1985). Ord Basin. Generally 75-80m thick; maximum of 210m thick in the type section in northeastern DIXON RANGE map area. Intertidal sand- and mudflat deposits. Broadly correlated with Jinduckin Formation-Oolloo Dolostone interval (Daly Basin); Point Wakefield beds (Wiso Basin); Anthony Lagoon Formation/Wonarah Formation/Ranken Limestone/Camooweal Dolostone succession (Georgina Basin).||Elder Subgroup.||Conformably and gradationally overlies Panton Formation. Is overlain conformably and gradationally by Overland Sandstone. Correlated with Hart Spring Sandstone (Bonaparte Basin).|Fine to medium feldspathic to micaceous, red-brown to maroon sandstone; minor siltstone, mudstone; trough cross-beds, ripple marks, parallel lamination, mud pebble and cobble moulds, decimetre-scale channels, dessication cracks, arthropod tracks.|12-JUL-16
23567|Eagle Hawk Sandstone|69634|4|Described|GEOL_LUT_CSV files|Furongian|Furongian|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|497-485.4 Ma (Biostrat)|Unit of Elder Subgroup.|||Red micaceous feldspathic sandstone; minor siltstone|
23567|Eagle Hawk Sandstone|69673|5|Briefly described|p194|||210m thick.||Elder Subgroup||Overlies Panton Formation, overlain by Overland Sandstone|Feldspathic to micaceous sandstones with minor siltstone and mudstone.|
23567|Eagle Hawk Sandstone|70154|5|Briefly described|100k_interpgeop_lut.csv|Ordovician|Cambrian||485-497 Ma|Elder Subgroup|||Red micaceous feldspathic sandstone; minor siltstone.|
23567|Eagle Hawk Sandstone|71267|4|Described|GEOL_LUT_CSV files|Furongian|Furongian|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny (450-295 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|497-485.4 Ma (biostrat)|Unit of Elder Subgroup.|||Fine to medium micaceous and feldspathic sandstone; minor siltstone and mudstone.|
23567|Eagle Hawk Sandstone|71800|4|Described|p25-p27|Late Cambrian|Middle Cambrian|Ord Basin. Deposited on an intertidal sand flat.||Elder Subgroup||Conformably (gradationally) overlies the Panton Formation. Overlain by the Overland Sandstone.|Red micaceous arkose.|
23567|Eagle Hawk Sandstone|73255|6|Mentioned|p534 Fig.2|Cambrian|Cambrian|||Goose Hole Group||Overlies the Panton Formation, underlies the Overland Sandstone.||
37105|Eastern Leucocratic Granitoid|23751|6|Mentioned|p13|||||||||
37105|Eastern Leucocratic Granitoid|60724|5|Briefly described|p10|||Of the Tickalara Metamorphics.||||||
27268|Eaton Sand|40367|2|Defined|p72, p76|Pleistocene|Pleistocene|Conformable overlies Tamala Limestone; grades up into Leschenault Fm.  Max. thickness: >10m. Of laminated to bedded yellow to orange qtz sand, med.+ coarse sand-sized grains; interstitial fine sand, minor clay||||||07-AUG-07
27268|Eaton Sand|40400|6|Mentioned|p109|||Of Semeniuk (1983). Geological Province: Perth Basin.||||||06-AUG-07
27268|Eaton Sand|40401|6|Mentioned|p128|||||||||
27268|Eaton Sand|41504|6|Mentioned|p71|||||||||
27268|Eaton Sand|42009|5|Briefly described|p75|||||||||
27268|Eaton Sand|73206|6|Mentioned|p856|Pleistocene|Pleistocene|Of Semeniuk (1983,1997). Overlain by Mandurah-Eaton Ridge [landform].||||||
78998|Edamurta Gabbro|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton. The two facies are mapped separately.|c.2795 Ma.|Annean Supersuite.|||Metagabbro, locally with relict igneous texture or garnet-bearing, deformed, greenschist to amphibolite facies. Anorthosite to leucogabbro with distinctive euhedral plagioclase megacrysts to 20mm long; metamorphosed.|
78998|Edamurta Gabbro|70796|5|Briefly described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. See also 100K_interpgeop_lut.csv, 500k_interpgeop_lut.csv. Numerous additional lithologies are discussed.|ca 2820 to 2735 Ma (inferred)|Annean Supersuite|||Metagabbro, typically deformed with greenschist to amphibolite facies; locally with relict igneous texture; locally garnetbearing. Anorthosite to leucogabbro with distinctive euhedral plagioclase megacrysts up to 20 mm long; metamorphosed.|
78998|Edamurta Gabbro|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.|2820-2735 Ma (inferred)|Unit of Annean Supersuite.|||Anorthosite to leucogabbro with distinctive euhedral plagioclase megacrysts; metamorphosed; metagabbro, typically deformed with greenschist to amphibolite facies assemblages; locally with relict igneous texture; locally garnet-bearing.|
75622|Eddy Suite|67380|5|Briefly described|p5, p8, p22|Statherian|Statherian|Biranup Zone, Albany-Fraser Orogen. These intrusions show increasing juvenile mantle-derived input through time, on both and inter-intrusion (>10 Ma) and intra-grain (<5 Ma) scale.|1665 +/- 4 Ma (Kirkland et al., 2009, 2010).||||Granitic and gabbroic rocks with distinct mingling and hybridisation textures. Includes megacrystic metamonzogranite, and equigranular metasyenogranitic gneiss, rapakivi-textured metagranodiorite and metagabbronorite.|
75622|Eddy Suite|68186|4|Described|p14,p18-19,p22,p38-39,p54-59, Plate 1A|Proterozoic|Proterozoic|Eastern Biranup Zone; well-exposed W of Harris Lake. The youngest rocks reflect a progressively more juvenile influence (?renewed back-arc extension). Occurs within a NE-trending, wedge-shaped fault slice. Lithologies, deformation and geochronology described in some detail.|c.1665-1660 Ma.||||Heterogeneously deformed pegmatites and granites. Ranges from megacrystic metamonzogranite and equigranular metasyenogranitic gneiss, to rapakivi-textured metagranodiorite and metagabbronoritic rocks. Inferred hybrid products. A-type.|
75622|Eddy Suite|69003|5|Briefly described|p4, p29-30|Paleoproterozoic|Paleoproterozoic|Albany-Fraser Orogen. Associated with the Biranup Orogeny.|c.1665-1660 Ma.||||Norite and granodiorite.|
75622|Eddy Suite|69386|5|Briefly described|p4, p31, p37|Proterozoic|Archean|Biranup Zone, Albany-Fraser Orogen. Associated with an anomalous (>18.3) rare earth element index sample in the Zanthus area.|||||Metagranodiorite, metagabbro and granitic gneiss.|
75622|Eddy Suite|69595|4|Described|p6, p14, p18, p54|Statherian|Statherian|Comprises the most isotopically juvenile magmas in the Biranup Zone.|1627 +/- 4 Ma (GSWA 194736) -1655 Ma||||Megacrystic metamonzogranite and equigranular metasyenogranitic gneiss, to rapikivi-textured, mingled metagranodiorite and metagabbronorite.Granitic and gabbroic-intermediate dykes also occur.|
75622|Eddy Suite|70084|5|Briefly described|p220|Statherian|Statherian|Geological province: Albany-Fraser Orogen, Yilgarn Craton. Associated with Biranup Orogeny and formation of the Barren Basin.||||||
75622|Eddy Suite|70090|6|Mentioned|p445, 458|Statherian|Statherian|Comprises mingled granitic and gabbroic intrusions. [Is this the same unit as Eddy Schist described in the rest of the text?] Associated with 1710-1650 Ma Biranup Orogeny.|c.1665 Ma|||||08-AUG-19
75622|Eddy Suite|70153|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic||1800 - 1625 Ma (inferred).||||Metagranodiorite, metadiorite and metagabbro, granitic gneiss, lenses of metasedimentary rocks, and pegmatite; may include remnants of other Biranup Zone units.|
75622|Eddy Suite|70182|5|Briefly described|p5, p21-24, p27-30, p32, p34, p39-40|||Eastern Biranup Zone, Albany-Fraser Orogeny. Compositionally coherent group of granites; part of a bimodal magmatic association (geochemistry detailed).|c.1665 Ma.||||Includes rapakivi-textured metagranodiorite mingled with metagabbro.|
75622|Eddy Suite|70802|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Kepa Kurl Booya Province, Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage I (1330-1260 Ma); Albany-Fraser Orogeny Stage II (1225-1140 Ma); Biranup Orogeny (1710-1620 Ma). See 500k_interpgeop14_lut.csv, 250k_pre_mesozoic_interpgeop_lut.csv.|1800-1625 Ma (inferred)||||Metagranodiorite, metadiorite and metagabbro, granitic gneiss, lenses of metasedimentary rocks, and pegmatite; may include remnants of other Biranup Zone units|
75622|Eddy Suite|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Kepa Kurl Booya Province, Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage II (1225 - 1140 Ma); Albany-Fraser Orogeny (1330 - 1140 Ma); Albany-Fraser Orogeny Stage I (1330 - 1260 Ma); Biranup Orogeny (1710 - 1620 Ma). See 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|1671+\-8 Ma; 1660+\-6 Ma||||Metagranodiorite, metadiorite and metagabbro, granitic gneiss, lenses of metasedimentary rocks, and pegmatite|
75622|Eddy Suite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Biranup Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen.|Max age 1671+/-8 Ma, min age 1660+/-6 Ma||||Metagranodiorite, metadiorite and metagabbro, granitic gneiss, lenses of metasedimentary rocks, and pegmatite.|
34906|Edmund Group|22897|6|Mentioned|102|||Geol province Bangemall Basin||||||
34906|Edmund Group|22905|4|Described|p52 Fig. 2, p53|Mesoproterozoic|Mesoproterozoic|Supersedes Edmund Subgroup.  Unconformably overlain by the Collier Group, and rocks of the Gascoyne Complex.  Max. thickness: ~3900m.||||||24-JAN-06
34906|Edmund Group|23403|4|Described|p6|Mesoproterozoic|Mesoproterozoic|Age: ~1462 +/- 3Ma.||||||
34906|Edmund Group|23485|4|Described|p30|Mesoproterozoic|Paleoproterozoic|Formerly Edmund Subgroup. Of Bangemall Supergroup. Geological Province: Edmund Basin.||||||07-NOV-08
34906|Edmund Group|23486|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Bangemall Supergroup. Geological Province: Edmund Basin.||||||07-NOV-08
34906|Edmund Group|23487|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Bangemall Supergroup. Geological Province: Edmund Basin.||||||07-NOV-08
34906|Edmund Group|23525|4|Described|p29|Mesoproterozoic|Paleoproterozoic|Of the Bangemall Supergroup. Geological Province: Edmund Basin.||||||07-NOV-08
34906|Edmund Group|23527|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Bangemall Supergroup, Edmund Basin||||||
34906|Edmund Group|23529|5|Briefly described|p7|||Geological Province: Bangemall Basin||||||
34906|Edmund Group|23620|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|Sandstone, siltstone, shale, dolomite, and chert: intruded by dolerite dykes and sills.  Of the Bangemall Supergroup.  See also p4 Fig. 4.||||||07-NOV-08
34906|Edmund Group|23780|5|Briefly described|p13|Proterozoic|Proterozoic|Of the Bangemall Supergroup.||||||
34906|Edmund Group|23781|5|Briefly described|p62|Mesoproterozoic|Mesoproterozoic|Of Bangemall Supergroup. Geological Province: Edmund Basin.||||||08-SEP-08
34906|Edmund Group|23976|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
34906|Edmund Group|23977|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
34906|Edmund Group|23978|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
34906|Edmund Group|24017|5|Briefly described|p8 Tb. 2, p23|Mesoproterozoic|Paleoproterozoic|Of the Bangemall Supergroup.  Geological Province: Edmund Basin.||||||07-NOV-08
34906|Edmund Group|24115|4|Described|p2, p27|Mesoproterozoic|Mesoproterozoic|Of the Bangemall Supergroup. Age: 1679 Ma - 1465 Ma. Unconformably overlies Palaeoproterozoic rocks of the Ashburton and Bresnahan Basins in the north, and the Gascoyne Complex in the south. Overlain by the Collier Group. Geological Province: Edmund Basin||||||
34906|Edmund Group|24161|5|Briefly described|p7|Paleoproterozoic|Paleoproterozoic|Age: 1620 - 1465 Ma. Geological Province: Edmund Basin.||||||07-NOV-08
34906|Edmund Group|24183|2|Defined|p1, p6, p7|Calymmian|Statherian|Thickness: >4000m. Unconformably overlies the Wyloo, Bresnahan, Mount Minnie and Padbury Groups and Gascoyne Complex. Unconformably overlain by the Collier Group. maximum age constrained by underlying granitoid rocks of the Gascoyne Complex (1670-1620 Ma). Minimum age from dolertie sills (1462 +/- 3 Ma) intruding the Ullawarra Formation.||||||21-MAR-11
34906|Edmund Group|24410|5|Briefly described|p137 Fig. 80|Proterozoic|Proterozoic|?Includes the Mount James Formation and Morrisey Metamorphic Suite; shale, sandstone, conglomerate and dolomite.||||||24-JUN-13
34906|Edmund Group|24522|6|Mentioned|p80 Fig. 2|||Geological Province: Bangemall Basin (WA).||||||
34906|Edmund Group|24535|4|Described|p2|Mesoproterozoic|Mesoproterozoic|Of the Bangemall Supergroup. Deposited between 1465 (dolerite sills intruding) and 1619+/-15 Ma (underlying monzogranite of Gascoyne Complex). Geological Province: Edmund Basin.||||Overlain by Collier Group.||26-NOV-13
34906|Edmund Group|24544|4|Described|p6|Paleoproterozoic|Paleoproterozoic|Quartz sandstone, conglomerate, siltstone and dolostone. Of the Bangemall Supergroup.||||||07-NOV-08
34906|Edmund Group|50008|5|Briefly described|p47 Fig.4|Mesoproterozoic|Mesoproterozoic|Of Bangemall Supergroup.||||||
34906|Edmund Group|50010|5|Briefly described|p53, 54|Mesoproterozoic|Mesoproterozoic|Age: c. 1465 Ma. Unconformably overlain by Collier Group. Of Bangemall Supergroup.||||||
34906|Edmund Group|50188|5|Briefly described|p9, p14|Paleoproterozoic|Paleoproterozoic|Age: 1640Ma (U-Pb SHRIMP, Nelson 1995). Contains Kiangi Creek Formation and ?Discovery Formation.||||||07-NOV-08
34906|Edmund Group|50218|5|Briefly described|p240 Fig.2|||Of the Bangemall Supergroup. Quartz sandstone, conglomerate, siltstone, dolostone. Geological Province: Edmund Basin.||||||07-FEB-11
34906|Edmund Group|50219|5|Briefly described|p260 Fig. 2|||Of the Bangemall Supergroup.  Quartz sandstone, conglomerate, siltstone and dolostone. Geological Province: Edmund Basin.||||||07-FEB-11
34906|Edmund Group|50222|5|Briefly described|p334 Tb. 2||Paleoproterozoic|Age: 1.64Ga. Geological Province: Edmund Basin.||||||07-NOV-08
34906|Edmund Group|50225|4|Described|p386 Fig. 1, p390|||Of the Bangemall Supergroup.  Unconformably overlies the Gascoyne Complex, Wyloo and Capricorn Groups; unconformably overlain by the Collier Group.  Age: c.1620-1465Ma.  Geological Province: Collier Basin.  See also p407.||||||07-FEB-11
34906|Edmund Group|50226|5|Briefly described|p416, p426, p427 Fig. 6|Mesoproterozoic|Mesoproterozoic|Of the Bangemall Supergroup.  Consists mainly of siltstone, dololutite, stromatolitic dolomite and sandstone.  Overlies the Wyloo Group and Gascoyne Complex; unconformably overlain by Collier Group.  Geological Province: Bangemall Basin.||||||
34906|Edmund Group|50292|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Bangemall Supergroup.  Geological Province: Edmund Basin.||||||07-NOV-08
34906|Edmund Group|50312|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Bangemall Supergroup. Geological Province: Edmund Basin.||||||07-NOV-08
34906|Edmund Group|50313|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Bangemall Supergroup.  Geological Province: Edmund Basin.||||||07-NOV-08
34906|Edmund Group|50380|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Bangemall Supergroup. Geological Province: Edmund Basin.||||||07-NOV-08
34906|Edmund Group|60301|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Bangemall Supergroup. Geological Province: Edmund Basin. Age: c. 1620Ma-c.1465Ma.||||||07-NOV-08
34906|Edmund Group|60535|5|Briefly described|p556|Mesoproterozoic|Mesoproterozoic|Age: ca 1465 Ma. Of the Bangemall Supergroup.||||||
34906|Edmund Group|61262|5|Briefly described|p458 App.|||At base of Bangemall Supersuite - overlies Durlacher Supersuite. Together with the Collier Group it overlies the Gascoyne Complex. See also p454.||||||18-JAN-07
34906|Edmund Group|61850|5|Briefly described|p324 Fig. 1||Proterozoic|Includes Discovery Chert. Of the Bangemall Supergroup. Sandstone, siltstone, mudstone, sandstone, dolomite, chert, conglomerate.||||||24-JUN-13
34906|Edmund Group|63246|5|Briefly described|p478 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Bangemall Supergroup.||||||
34906|Edmund Group|63469|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Of Bangemall Supergroup. Includes; Kiangi Creek Formationand Irregully Formation.  Intruded by Narimbunna Dolerite.||||||24-SEP-07
34906|Edmund Group|63470|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Of the Bangemall Supergroup.  Age: <1620Ma. Intruded by Narimbunna Dolerite (sills). Geological Province: Edmund Basin.  Includes; Yilgatherra, Irregully, Blue Billy, Kiangi Creek, Discovery, Devil Creek and Ullawarra Formations.||||||07-NOV-08
34906|Edmund Group|63471|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Of the Bangemall Supergroup. Geological Province: Edmund Basin.||||||07-NOV-08
34906|Edmund Group|63866|4|Described|p152-p155, p157|Mesoproterozoic|Late Palaeoproterozoic|At least 4km thick. This group is interpreted as older than 1465 (Wingate, 2002) and younger than the 1619 +/- 15 Ma monzogranite in the underlying Gascoyne Complex. See also p162-p164, p168, p175-p176.|c. 1640 Ma (inferred, unit relationship)||Includes the Yilgatherra, Irregully, Gooragoora, Blue Billy, Cheyne Springs, Kiangi Creek, Muntharra, Discovery, Devil Creek, Ullawarra, Coodardoo and Coobarra Formation.|Overlies the Capricorn Group and the Padbury Group. Unconformably overlies the Mount James Formation. Disconformably overlain by the Collier Group.|Fine-grained siliciclastic and carbonate sedimentary rocks.|
34906|Edmund Group|63869|4|Described|p1, p4, p5, p11, p12, p14, p15, p24|Mesoproterozoic|Paleoproterozoic|See also p26-39, p42-47, p48, p51-53, Plate 1. Martin and Thorne, (2002); formerly Edmund Subgroup (of Bangemall Group). Edmund Basin. Over 4 km thick. Intruded by two suites of dolerite sills: one aged 1465 Ma and another aged 1070 Ma.|Between 1620-c.1465 Ma.|Unit in Bangemall Supergroup.|Includes Coobarra, Yilgatherra, Irregully, Gooragoora, Blue Billy, Cheyne Springs, Kiangi Creek, Muntharra, Discovery, Devil Creek, Ullawarra and Coodardoo Formations.|Unconformably overlies Gascoyne Complex and Wyloo Group. Is overlain unconformably by Collier Group.|Mostly fine-grained siliciclastic and carbonate sedimentary rocks: siltstone, sandstone, conglomerate, dolostone, stromatolitic dolostone, carbonaceous siltstone, chert; thick dolerite and gabbro sills.|
34906|Edmund Group|64283|5|Briefly described|p50 Fig. 1|Mesoproterozoic|Paleoproterozoic|Of the Bangemall Supergroup. Age: <1645Ma. Probably correlates with Cornelia Sandstone and Quadrio Formation.||||||07-FEB-11
34906|Edmund Group|64286|6|Mentioned|p74 Tb. 1|Mesoproterozoic|Paleoproterozoic|Age: c.1.6Ga. See also Table 1.||||||07-FEB-11
34906|Edmund Group|64287|5|Briefly described|p31|||Lowermost in the Bangemall Supergroup. Includes Irregully Formation. Unconformably overlain by Collier Group. Geological Province: Jillawarra Sub-basin.||||||07-FEB-11
34906|Edmund Group|64580|4|Described|map legend|Mesoproterozoic|Paleoproterozoic|Sandstone, siltstone, mudstone, dolostone, and chert; minor conglomerate.||||||15-DEC-08
34906|Edmund Group|64722|5|Briefly described|p7||Statherian|Of Mesoproterozoic Edmund Basin. Sediment thought to be sourced from the West Australian Craton, including Gascoyne Complex and equivalent basins of Capricorn Orogen and southern Pilbara Craton.||Lower unit of  Bangemall Supergroup.||Unconformably overlain by Collier Group.||11-APR-12
34906|Edmund Group|64724|5|Briefly described|p45 Fig.5, p48|Calymmian|Statherian|Maximum age constrained by zircon xenocrysts in rhyolites at its base (1638 +/- 14 Ma). Minimum age from intruding dolerite sills (1465 +/- 3 Ma).||||||02-APR-12
34906|Edmund Group|64728|5|Briefly described|pp93-95, p108.|Mesoproterozoic|Mesoproterozoic|Edmund Basin. Records erosion of Gascoyne Province and progressive unroofing of Paleoproterozoic supracrustal rocks on southern Pilbara Craton margin. Intruded by dolerite sills aged c.1465 Ma.||Lower unit in Bangemall Supergroup.|Includes Yilgatherra, Irregully, Blue Billy, Cheyne Springs, Gooragoora, Kiangi Creek, Muntharra, Discovery, Devil Creek, Ullawarra and Coodardoo Formations.|Unconformably overlies Collier Group.||
34906|Edmund Group|64772|5|Briefly described|p9, p13,  p14 Fig.7, p20-21 Fig.10|Mesoproterozoic|Paleoproterozoic|Superseded Edmund Subgroup when Bangemall Basin stratigraphy was reviewed (Martin et al (1999). Age: 1620-1465Ma. Correlated with Scorpion Group.||||||25-NOV-13
34906|Edmund Group|64777|5|Briefly described|p6-7|Mesoproterozoic|Mesoproterozoic|Intruded by dolerite sills with SHRIMP U-Pb zircon and baddeleyite ages of 1465 and 1070 Ma (Wingate 2002). Includes detrital zircons of 1780 Ma.(Nelson 2002)|>1465 Ma|Of the Bangemall Supergroup||||
34906|Edmund Group|64872|6|Mentioned|p25, p24 Fig.1|Mesoproterozoic|Mesoproterozoic|Unit in Bangemall Supergroup. Low-grade slates. The base is locally intruded by carbonatitic rocks and ultramafic lamprophyres.||||||
34906|Edmund Group|65152|5|Briefly described|p2 Fig.1, p3.|Mesoproterozoic|Mesoproterozoic|Unit in Bangemall Supergroup. Fine-grained siliciclastic sediments and carbonates. Folding and low-grade metamorphism caused by Edmundian Orogeny.||||||01-MAY-15
34906|Edmund Group|65450|5|Briefly described|p1, p2 Fig.1, p3-5, p6 Fig.4, p27|Mesoproterozoic|Mesoproterozoic|Edmund Basin. Dolerite sill intrusion dated at around 1465 Ma.|Max: 1620 Ma, min: c. 1465 Ma|Bangemall Supergroup|Discovery Formation, Kiangi Creek Formation, Yilgatherra Formation|Unconformably overlies Padbury Group.|Low grade meta-sedimentary rocks.|
34906|Edmund Group|65453|5|Briefly described|map legend|Mesoproterozoic|Paleoproterozoic|Of Bangemall Supergroup. Includes Ullawarra, Devil Creek, Discovery, Kiangi Creek, Irregully and Yilgatherra Formations. Intruded by Narimbunna Dolerite. Faulted against Mount Augustus Sandstone. Geol. Prov: Edmund Basin.||||||
34906|Edmund Group|65506|5|Briefly described|p986-988, p990-999|||3900m thick, siliciclastic and carbonate rocks. Overlain unconformably by Collier Group. Narimbunna Dolerite in between Collier Group and Edmund Group. Part of Bangemall Supergroup. Detailed geochemistry of sills.||||||
34906|Edmund Group|65545|5|Briefly described|Map Legend|Mesoprotoerozoic|Paleoproterozoic|Of Bangemall Supergroup, Edmund Basin. Age: c. 1460 - <1620 Ma. Includes Ullawarra, Devil Creek, Discovery, Kiangi Creek, Irregully, and Yilgatherra Formations. ||||||
34906|Edmund Group|65549|5|Briefly described|Map Legend|Calymmian|Statherian|Of the Bangemall Supergroup, Edmund Basin. Sedimentary group of the Edmund Basin that includes Ullawarra, Devil Creek, Discovery, Kiangi Creek, Irregully, Yilgatherra formations. Shown as younger than Durlacher Supersuite of the Gascoyne Province.||||||07-SEP-10
34906|Edmund Group|65830|3|Fully described|p1-2, p4, p5, p8-17, p19, p21, p25-26|Calymmian|Statherian|See also p28, p34, p38, Plate 1. ~ 4km thick. Younger than the 1680-1620 Ma granites in the underlying Gascoyne Complex, and older than the 1465 Ma dolerite sills that intrude it over large areas of EDMUND 1:100,000 map sheet.|Between 1620 and c.1465 Ma.|Of the Bangemall Supergroup|Includes Yilgatherra, Irregully, Gooragoora, Blue Billy, Cheyne Springs, Kiangi Creek, Muntharra, Discovery, Devil Creek, Ullawarra and Coodardoo Formations.|Unconformably underlain  by the Bresnahan Group. Underlain by the Gascoyne Complex. Unconformably overlain by the Collier Group.|Sedimentary rocks.|
34906|Edmund Group|65896|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Lower part of Bangemall Supergroup, Edmund Basin. 1620 - 1465 Ma. Includes (in ascending order) Tringadee, Irregully, Kiangi Creek, Discovery, Devil Creek and Ullawarra Formations. Intruded by dolerite and gabbro sills dated from c. 1465 Ma to c. 1070 Ma.||||||
34906|Edmund Group|66104|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Lower part of Bangemall Supergroup, Edmund Basin. Age shown as 1620 - 1465 Ma. Includes (in ascending order) Irregully, Kiangi Creek, Discovery, Devil Creek and Ullawarra Formations. Intruded by dolerite and gabbro sills of the Narimbunna Dolerite.||||||
34906|Edmund Group|66105|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin. Unit in Bangemall Supergroup. Includes Ullawarra, Devil Creek, Discovery, Kiangi Creek, Irregully and Yilgatherra Formations. Intruded by Narimbunna Dolerite. Age ranges from <1620 Ma to c.1465 Ma.||||||06-OCT-11
34906|Edmund Group|66107|5|Briefly described|p4 Fig.1, p5 |Mesoproterozoic|Mesoproterozoic|Minimum age constrained by intrusions.|c.1465 Ma minimum.|||Unconformably overlain by the Collier Group.|Shale, sandstone, dolomite.|
34906|Edmund Group|66110|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in Bangemall Supergroup. Includes Yilgatherra, Irregully, Kiangi Creek, Discovery, Devil Creek and Ullawarra Formations. Age ranges from <1620 Ma to c.1465 Ma. Intruded by dolerite and gabbro sills of the Narimbunna Dolerite.||||||
34906|Edmund Group|66112|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in Bangemall Supergroup. Edmund Basin. Aged c.1620 to c.1460 Ma. Includes Yilgatherra, Irregully, Kiangi Creek, Discovery, Devil Creek and Ullawarra Formations, several of which have unnamed units. Intruded by Narimbunna and Kulkatharra Dolerites.||||||
34906|Edmund Group|66241|4|Described|pp1-4, p9, pp28-29. |Mesoproterozoic|Paleoproterozoic|Edmund Basin. |c.1620 Ma to >1465 Ma.|Basal unit in Bangemall Supergroup.|Includes Yilgatherra, Irregully, Gooragoora, Blue Billy, Cheyne Springs, Kiangi Creek, Muntharra, Discovery, Devil Creek, Ullawarra and Coodardoo Formations.|Is overlain disconformably by Collier Group.|Fine- to coarse-grained siliciclastic and carbonate sedimentary rocks; minor felsic volcanic rocks.|
34906|Edmund Group|66299|4|Described|p51, p145, pp202-207.|Mesoproterozoic|Mesoproterozoic|Intruded by sills of Narimbunna and Kulkatharra Dolerites, and Mundine Well Dolerite Suite. |Maximum 1620 Ma.|Unit in Bangemall Supergroup.|Includes basal unit Yilgatherra Formation, Irregully, Kiangi Creek, Discovery, Devil Creek and Ullawarra Formations.|Unconformably overlies Moorarie Supersuite, Biddenew Formation and Durlacher Supersuite.|Slates, sandstones.|
34906|Edmund Group|66427|6|Mentioned|p40 Fig.1|||Intruded by dolerite sills c.1.46 Ga; deformed <1.46-1.22 Ga.|1.64 Ga.|||||
34906|Edmund Group|66579|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin||Shown as only unit in Bangemall Supergroup.|Includes Yilgatherra and Irregully Formations, as well as an unnamed unit of sandstone, conglomerate, siltstone and dolostone.||Clastic and carbonaceous sediments.|
34906|Edmund Group|66887|5|Briefly described|p3 Fig.2, p5 Fig.4, p7|Mesoproterozoic|Mesoproterozoic|Southern Gascoyne Province.|~1570-~1460 Ma estimated from Fig.4.||Yilgatherra Formation|||14-DEC-16
34906|Edmund Group|66950|6|Mentioned|p9 Fig.8|Calymmian|Calymmian||c. 1600-1400 Ma|||||
34906|Edmund Group|67136|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Unit in Bangemall Supergroup.|Includes Irregully, Blue Billy, Kiangi Creek, Discovery, Devil Creek, Ullawarra and Coodardoo Formations.|Overlies Bresnahan Group. Is intruded by Narimbunna Dolerite and Kulkatharra Dolerite sills.||
34906|Edmund Group|67245|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Edmund Basin.||Unit in Bangemall Supersuite.|Includes Yilgatherra, Irregully, Kiangi Creek, Discovery, Devil Creek and Ullawarra Formations.|Overlies Moorarie Supersuite. Is intruded by Narimbunna Dolerite.||
34906|Edmund Group|67246|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Edmund Basin. ||Unit in Bangemall Supergroup.|Includes Yilgatherra, Irregully, Kiangi Creek, Discovery, Devil Creek and Ullawarra Formations.|Overlies nonconformably Moorarie Supersuite. Is intruded by Narimbunna Dolerite.||
34906|Edmund Group|67247|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Edmund Basin.|<1620 Ma.|Unit in Bangemall Supergroup.|Includes Yilgatherra, Kiangi Creek and Irregully Formations.|||
34906|Edmund Group|67269|5|Briefly described|p20-21 Fig.19|Calymmian|Statherian|Bangemall Basin.|1620-1465 Ma.||Kiangi Creek Formation.|||
34906|Edmund Group|67346|5|Briefly described|p793, p794 Fig.1, p795 Fig.2, p796 Fig.3|Mesoproterozoic|Mesoproterozoic|Edmund and Collier Basins.|||Includes Discovery, Kiangi Creek, Yilgatherra, Devil Creek and Ullawarra Formations.|Unconformably underlain by correlates of Padbury Group.||11-MAY-12
34906|Edmund Group|67371|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Edmund Basin.||Unit in Bangemall Supergroup.|Includes Yilgatherra and Irregully Formations.||Sandstones, conglomerate, dolostones, siltstones.|
34906|Edmund Group|67374|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Unit in Bangemall Supergroup.|Includes Irregully, Blue Billy, Cheyne Springs, Kiangi Creek, Discovery, Devil Creek, Ullawarra and Coodardoo Formations.|Intruded by sills of Narimbunna and Kulkatharra Dolerites.|Sandstones, mudstone, dolostone, conglomerate, chert.|01-NOV-12
34906|Edmund Group|67843|6|Mentioned|p2 Fig.1, p4, p13. |Mesoproterozoic|Mesoproterozoic|Deposition was intermittently controlled by the Talga Fault. Sedimentary protoliths were metamorphosed and deformed during the 1030-955 Ma Edmundian Orogeny.||||||
34906|Edmund Group|67888|5|Briefly described|p54|Mesoproterozoic|Paleoproterozoic||1620-1465 Ma|Bangemall Supergroup||Overlain by Collier Group|Quartz-muscovite schists.|
34906|Edmund Group|68280|6|Mentioned|p26 fig 24|||Bangemall Basin.|||Includes Kiangi Creek Formation|||
34906|Edmund Group|68285|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin. Age constrained by intrusion by Narimbunna Dolerite (c. 1465 Ma) and older Mangaroon Orogeny (1677-1619 Ma, Sheppard, 2005 AJES)|c. 1620-1460 Ma|Of the Bangemall Supergroup.|Includes the Coodardoo Formation, Ullawarra Formation, Devil Creek Formation, Discovery Formation, Kiangi Creek Formation, Cheyne Springs Formation, Blue Billy Formation, Irregully Formation.|Intruded by Kulkatharra Dolerite and Narimbunna Dolerite.||
34906|Edmund Group|68286|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin. Age constrained by intrusion by Narimbunna Dolerite (c. 1465 Ma) and older Mangaroon Orogeny (1677-1619 Ma, Sheppard, 2005 AJES)|c. 1620-1460 Ma|Of the Bangemall Supergroup.|Includes the Coodardoo Formation, Ullawarra Formation, Devil Creek Formation, Discovery Formation, Kiangi Creek Formation, Cheyne Springs Formation, Blue Billy Formation, Irregully Formation.|Intruded by the Kulkatharra Dolerite. Intruded by the Narimbunna Dolerite.||
34906|Edmund Group|68521|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|||Of the Bangemall Supergroup.|Includes Kiangi Creek Formation and Irregully Formation.|Intruded by the Narimbunna Dolerite.||
34906|Edmund Group|68522|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin.|<1620 - c.1465 Ma|Of the Bangemall Supergroup.|Includes Kiangi Creek Formation, Irregully Formation, and Yilgatherra Formation.|Intruded by the Narimbunna Dolerite.||
34906|Edmund Group|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv|Mesoproterozoic|Paleoproterozoic|500K_GEOLOGYP08_LUT.csv||Bangemall Supergroup|||sandstone, siltstone, mudstone, dolostone, and chert; minor conglomerate|
34906|Edmund Group|68981|5|Briefly described|p25|Mesoproterozoic|Mesoproterozoic|Edmund Basin. Metasedimentary rocks.||||Is intruded by Narimbunna Dolerite sills.||
34906|Edmund Group|69003|4|Described|p4, p9 Fig.9, p24, p33-36, p41-43, p56|Mesoproterozoic|Mesoproterozoic|Edmund Basin, Capricorn Orogen. Up to 5km thick. Sediments in the lower parts were sourced from Capricorn, Mount Minnie and Bresnahan Groups; the upper parts from Hamersley and Fortescue Groups. Underwent faulting and extensive hydrothermal alteration during the 1385-1200 Ma Mutherbukin Tectonic Event, and further folding and faulting during the 1030-955 Ma Edmundian Orogeny. Hosts the giant Abra polymetallic deposit.|||Yilgatherra, Irregully, Gooragoora, Blue Billy, Cheyne Springs, Kiangi Creek, Muntharra, Discovery, Devil Creek, Ullawarra and Coodardoo Formations.|Unconformably overlies Capricorn Group and Durlacher Supersuite. Is overlain by Collier Group.|Fine-grained siliciclastic and carbonate sedimentary rocks.|
34906|Edmund Group|69010|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Of the Bangemall Supergroup.|Includes the Ullawarra Formation.|Intruded by Kulkatharra Dolerite.||24-APR-14
34906|Edmund Group|69024|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin. Dolerite and gabbro sills intruded into the Edmund Group range in age from c. 1465 Ma (Sircombe, 2003; Nelson, 2001) to c. 1070 Ma (Sircombe, 2003; Nelson, 2001).||Of the Bangemall Supergroup.|Includes Ullawarra, Devil Creek, Discovery, Muntharra, Kiangi Creek, Cheyne Springs, Blue Billy, Gooragoora, Irregully and Yilgatherra Formations.|||05-MAY-14
34906|Edmund Group|69027|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin. Intruded by dolerite and gabbro sills from c.1465 Ma to c.1070 Ma (Wingate, 2002; Nelson 2004). See map legend for a detailed lithological description.||Of the Bangemall Supergroup.|Includes Coodardoo, Ullawarra, Devil Creek, Discovery, Muntharra, Kiangi Creek, Cheyne Springs, Blue Billy, Gooragoora, Irregully, and Yilgatherra Formations.|Overlain by the Collier Group. Underlain by the Wyloo Group.|Includes sandstone, siltstone, mudstone, dolostone, chert, dolomitic siltstone, dolorudite, and conglomerate; intrusive dolerite sills.|05-MAY-14
34906|Edmund Group|69028|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin.|1620-1465 Ma||Includes Discovery, Devil Creek, Ullawarra, Coodardoo, Kiangi Creek, Muntharra, Gooragoora, Blue Billy, Cheyne Springs, Yilgatherra, and Irregully Fomations.|Intruded by the Kulkatharra and Narimbunna Dolerites.|Includes siltstone and mudstone; sandstone, dolomitic mudstone, chert, and minor conglomerate; stromatolitic and non-stromatolitic dolostone.|06-MAY-14
34906|Edmund Group|69080|4|Described|p684, p690-692, p694-697, p699, p701|Calymmian|Statherian|Gascoyne Province. Detritus sourced predominantly from Fortescue and Hamersley Groups. Age range 1620-1465 Ma. Seismic architecture described. Hosts the polymetallic Pb-Cu-Zn deposit at Abra, associated with the Lyons River Fault.|1463 +/- 8 Ma (Wingate et al., 2010).|||Unconformably overlies Durlacher Supersuite. Intruded by Kulkatharra Dolerite sills.|Mixed siliciclastic and carbonate sedimentary rocks; minor volcanic rocks.|
34906|Edmund Group|69091|6|Mentioned|p181||Paleoproterozoic|Maximum depositional ages of ~1800-1770 Ma, were reported for some samples by Martin et al. (2008).||||||
34906|Edmund Group|69166|5|Briefly described|geologyp_lut.csv|Mesoproterozoic|Paleoproterozoic|Also includes the Irregully Formation, Kiangi Creek Formation, Tangadee Rhyolite, Ullawarra Formation, Muntharra Formation, Cheyne Springs Formation,Devil Creek Formation, Yilgatherra Formation, Tringadee Formation.||Bangemall Supergroup|Includes Blue Billy Formation, Coodardoo Formation, Discovery Formation, Gooragoora Formation|Unconformably overlies Spring Camp Formation|Undivided, sandstone, siltstone, mudstone, dolostone, and chert; minor conglomerate.|
34906|Edmund Group|69185|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Paleoproterozoic|Of Edmund Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.||Unit of Bangemall Supergroup.|Includes Blue Billy, Cheyne Springs, Coodardoo, Devil Creek, Discovery, Gooragoora, Irregully, Kiangi Creek, Muntharra, Ullawarra and Yilgatherra formations.||Siltstone and mudstone (in part dolomitic); sandstone, stromatolitic and non-stromatilitic dolostone; locally sulfidic, dolomitic mudstone, chert, minor conglomerate.|
34906|Edmund Group|69237|6|Mentioned|p2, p4|Mesoproterozoic|Mesoproterozoic|||Bangemall Supergroup.||||
34906|Edmund Group|69387|5|Briefly described|p16-19, p21-35, p50|Calymmian|Statherian|Gascoyne Province. Structural fabric diagrams; deformation discussed. SG and magnetic susceptibility values given. Gravity and magnetic modelling.|1620-1465 Ma.|||Is intruded by Narimbunna Dolerite.||
34906|Edmund Group|69546|6|Mentioned|p102,106|Mesoproterozoic|Mesoproterozoic|Geological province: Gascoyne Province.||||||
34906|Edmund Group|69583|5|Briefly described|p130, Plate 3.|Mesoproterozoic|Mesoproterozoic|Edmund Basin.|1620-1465 Ma.||Yilgatherra, Irregully Formations.||Stromatolitic and non-stromatolitic dolostone, dolomitic silstone, sandstone, siltstone and conglomerate.|
34906|Edmund Group|69596|5|Briefly described|p4-9, p12-13, p32-33|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen. Affected by the 1385-1170 Ma Mutherbukin Tectonic Event and the 1030-955 Ma Edmundian Orogeny.||Bangemall Supergroup.|Yilgatherra, Irregully, Gooragoora, Blue Billy, Cheyne Springs, Kiangi Creek, Muntharra, Discovery, Devil Creek, Ullawarra, Coodardoo Formations.|Unconformably overlies Moorarie Supersuite. Is intruded by Kulkatharra Dolerite.||
34906|Edmund Group|70019|4|Described|p91,93-94,108|Mesoproterozoic|Mesoproterozoic|Geological province: Gascoyne Province, Capricorn Orogen. Folded by 1320-1170 Ma Mutherbukin Tectonic Event, and probably resulted in fault-reactivations and hydrothermal fluid activity c. 1220 Ma as recorded by hydrothermal monazite in Irregully Formation. Lower Edmund group depositional age is loosely constrained between c. 1680 and 1500 Ma; maximum depositional age is constrained by 1679+\-3 Ma detrital zircons from the Mt Augustus Sandstone.|||Includes Coodardoo, Ullawarra , Devil Creek, Discovery, Muntharra Formation, Kiangi Creek, Cheyne Springs, Blue Billy, Gooragoora, Irregully and Yilgatherra formations.|Overlain by Collier Group. Underlain unconformably, or in fault contact with Durlacher Supersuite.||
34906|Edmund Group|70127|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Bangemall Supergroup.|Yilgatherra, Irregully, Gooragoora, Kiangi Creek, Discovery, Devil Creek, Formations.|||
34906|Edmund Group|70132|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Bangemall Supergroup.|Irregully, Kiangi Creek, Discovery, Devil Creek and Ullawarra Formations.|Is intruded by Kulkatharra Dolerite.|Siltstone, sandstone, chert, dolostone, conglomerate.|
34906|Edmund Group|70136|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.|<1620 - > 1460 Ma.|Bangemall Supergroup.|Ullawarra Formation.|Is intruded by Kulkatharra Dolerite.||
34906|Edmund Group|70138|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Bangemall Supergroup.|Yilgatherra, Irregully, Gooragoora, Kiangi Creek, Discovery and Devil Creek Formations.|Overlies Pooranoo Metamorphics. Is intruded by Narimbunna Dolerite.||09-NOV-15
34906|Edmund Group|70767|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Bangemall Supergroup.|Irregully, Blue Billy, Kiangi Creek, Discovery, Devil Creek, Ullawarra Formations.|Unconformably overlies Bresnahan Group. Is overlain by Collier Group. Is intruded by Kulkatharra Dolerite.||
34906|Edmund Group|70768|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Bangemall Supergroup.|Irregully, Blue Billy, Kiangi Creek, Discovery, Devil Creek, Ullawarra Formations.|Unconformably overlies Bresnahan Group. Is overlain by Collier Group. Is intruded by Kulkatharra Dolerite.||
34906|Edmund Group|70795|6|Mentioned|100k_geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Also 2_5m_interpgeop15_lut.csv, West Australian Craton. Also includes the Discovery Formation, Muntharra Formation, Kiangi Creek Formation, Cheyne Springs Formation, Blue Billy Formation, Gooragoora Formation, Irregully Formation, Yilgatherra Formation, Tringadee Formation.|1455 Ma|Bangemall Supergroup|Includes Coodardoo Formation, Ullawarra Formation, Curran Member, Nanular Member, Devil Creek Formation|Intruded by Kulkatharra Dolerite, Narimbunna Dolerite, Overlain by Backdoor Formation, unconformably overlies Spring Camp Formation|Mixed siliciclastic and carbonate sedimentary rock, chert and minor volcanic rock.|
34906|Edmund Group|70796|5|Briefly described|500k_interpgeop14_lut.csv|Mesoproterozoic|Paleoproterozoic|Edmund Basin, Capricorn Oorgen, Edmund Fold Belt. Affected by the Edmundian and Paterson orogenies.|ca. 16201500 Ma|Bangemall Supergroup||Intruded by the Kulkatharra Dolerite.|Stromatolitic and nonstromatolitic dolostone, dolomitic siltstone, sandstone, siltstone, and conglomerate.|
34906|Edmund Group|70814|5|Briefly described|iii, iv, p2-p4, p5, p7, p10|Mesoproterozoic|Paleoproterozoic|Edmund Basin. Note ages are poorly constrained and as such the ages provided are considered to be tentative. Deposition, provenance and tectonic setting are discussed in detail. See also p15, p17-p21, p25-p30, p32, p33-p34, p37-p39, p41, p47, p49, p53. Intruded by the Waldburg, Narimbunna and Kulkatharra Dolerites. Faulted against the Discretion Granite.|ca 1679-1452 Ma||Includes the Yilgatherra, Irregully, Gooragoora, Blue Billy, Cheyne Springs, Kiangi Creek, Muntharra, Discovery, Devil Creek, Ullawarra and Coodardoo Formations.|Unconformably overlies the Dingo Creek, Pimbyana and Yangibana Granites. Overlies the Mount Augustus Sandstone.||04-MAY-23
34906|Edmund Group|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Edmund Basin. D eposited during the Capricorn Orogeny.||Bangemall Supergroup||Is intruded by the Waldburg and Narimbunna Dolerite Suites.||
34906|Edmund Group|70936|5|Briefly described|p61,74|Mesoproterozoic|Mesoproterozoic|Geological province: Pilbara Craton. Contains dolerite sills of c. 1465 Ma. Also contains c. 1800 Ma and c. 1650 Ma detrital zircon peaks.||Unit of Bangemall Supergroup.||Overlain unconformably by Collier Group.||
34906|Edmund Group|70949|6|Mentioned|p988|Mesoproterozoic|Mesoproterozoic|||||||
34906|Edmund Group|71000|6|Mentioned|p65|Mesoproterozoic|Mesoproterozoic|Southern Gascoyne Province.||||||
34906|Edmund Group|71003|6|Mentioned|p61, p74, p76|Mesoproterozoic|Mesoproterozoic|Pilbara Craton. The minimum age is derived from dating of dolerite sills which intersect this unit. This unit has detrital zircon peaks dated at c. 1800 Ma and c. 1650 Ma.|c. 1465 Ma (minimum age)|Bangemall Supergroup||Unconformably overlain by the Collier Group.||
34906|Edmund Group|71042|6|Mentioned|p66 fig 2|Mesoproterozoic|Mesoproterozoic|||||||
34906|Edmund Group|71158|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||||Is intruded by  Kulkatharra Dolerite.||
34906|Edmund Group|71169|5|Briefly described|p71|Calymmian|Calymmian|West Australian Craton. |c. 1600-1500 Ma|||||
34906|Edmund Group|71273|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin.|c.1679-c.1455 Ma.||Yilgatherra, Irregully, Kiangi Creek, Discovery, Devil Creek Formations.|Is intruded by Narimbunna Dolerite.||16-FEB-18
34906|Edmund Group|71484|5|Briefly described|p125|||Geological province:  Of Edmund and Collier basins. Intruded by Kulkatharra and Marimbunna dolerites.||Unit of Bangemall Supergroup.|||Silstone, mudstone, sandstone; dolostone, chert and conglomerate.|30-AUG-19
34906|Edmund Group|71803|6|Mentioned|p367 fig 1|||||||||
34906|Edmund Group|71804|5|Briefly described|p392, p402|||Gascoyne Province. Geochronology results, interpretation and methodology are discussed. Potentially derformed during the Mutherbukin Tectonic Event or the Edmundian Orogeny.|ca. 1680-1465 Ma|||||
34906|Edmund Group|71869|6|Mentioned|p3-p4|||Capricorn Orogen.|1679-1455 Ma|Bangemall Supergroup||||
34906|Edmund Group|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Paleoproterozoic|Edmund Basin. Shown as 4 informal separate depositional packages. Package 1 is considered Paleoproterozoic; Package 2 Paleoproterozoic to Mesoproterozoic; Packages 3, 4 both Mesoproterozoic. 1 Stromatolitic/non-stromatolitic dolostone, dolomitic siltstone, sandstone, siltstone, conglomerate. 2 Siltstone + mudstone; sandstone, dolostone; locally sulfidic. 3 Siltstone + mudstone; sandstone + dolostone, minor conglomerate. 4 Siltstone + mudstone; sandstone, dolostone, dolomitic mudstone, chert + minor conglomerate.||||Intruded by sills of Narimbunna Dolerite, Waldburg Dolerite.|1 Stromatolitic/non-stromatolitic dolostone, dolomitic siltstone, sandstone, siltstone, conglomerate. 2+3 Siltstone, mudstone; sandstone, dolostone, minor congl. 4 Siltstone + mudstone; sandstone, dolostone, dolomitic mudstone, chert + minor cong.|
34906|Edmund Group|72259|6|Mentioned|p3, p9|Calymmian|Statherian|U-Th-Pb monazite and xenotime ages of ca. 900-850 Ma (cf. Johnson et al., 2009) [metamorphic/metasomatic ages?].|||||Includes slate.|
34906|Edmund Group|72705|5|Briefly described|p1, 3-6, 8, 10-11, 14, 16|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen. Deposition was followed by two Low-T events:  Mutherbukin Tectonic Event (c.1320-1170 Ma) and Edmundian Orogeny (c.1030-009 Ma). The age range given is an MDA from a detrital zircon, and from a cross-cutting dolerite dyke. Intracratonic shelf to basinal deposits up to 5km thick. Metamorphosed to lower greenschist facies. Up-sequence change in sediment provenance discussed.|c.1679 Ma - c.1455 Ma.||Yilgatherra, Irregully, Gooragoora, Blue Billy, Cheyne Springs, Kiangi Creek, Muntharra, Discovery, Devil Creek, Ullawarra, Coodardoo Formations.|Unconformably overlies Durlacher Supersuite. Is overlain by Collier Group. Is intruded by Narimbunna Dolerite dyke.|Mainly fine-grained siliciclastic and carbonate sedimentary rocks; grouped into 4 packages representing progressive deepening during crustal extension.|
34906|Edmund Group|73102|5|Briefly described|p1, p3-4, p21-22|||Gascoyne Province. Hosts extensive dolerite sills of the Narimbunna Dolerite and Kulkatharra Dolerite.|||Gooragoora Formation, Ullawarra Formation.|Intruded by Kulkatharra Dolerite, Narimbunna Dolerite, Waldburg Dolerite.|Mixed siliciclastic and carbonate sedimentary rock, minor volcanic rock.|
34906|Edmund Group|73214|5|Briefly described|p974 Fig.1|Mesoproterozoic|Mesoproterozoic|Mapped in Fig. 1 as one unit with Collier Group. Affected by the 1320-1170 Ma Mutherbukin Event and the 1030-900 Ma Edmundian Orogeny.||||||
34906|Edmund Group|73442|5|Briefly described|p1, p3-4, p14-15, p20, p27|Proterozoic|Proterozoic|Capricorn Orogen. Unconformably overlies Gascoyne Province and the margins of Archean cratons. Intruded by mafic sills.|||Coodardoo Formation|Intruded by Waldburg Dolerite, Narimbunna Dolerite, Kulkatharra Dolerite|Mixed siliciclastic and carbonate sedimentary rock, minor volcanic rock. Low-grade, variably deformed.|
34906|Edmund Group|74493|5|Briefly described|p2, p3 Fig.2, p7|Calymmian|Statherian||1673-1455 Ma|||Unconformably overlies Pooranoo Metamorphics, Durlacher Supersuite|Sedimentary rocks.|
34906|Edmund Group|74494|5|Briefly described|p1008-1009, p1014, p1017, p1020|||Cross-cut by ironstone dykes of the Gifford Creek Carbonatite Complex.||||Intruded by Gifford Creek Carbonatite Complex|Metasedimentary rocks.|
35377|Edna May Gneiss|23200|4|Described|p1013, 1014||Archean|Tonalitic orthogneiss.||||||07-NOV-08
35377|Edna May Gneiss|23201|4|Described|p1021, Fig.2||Archean|Age: 2.8Ga. Tonalitic Gneiss.||||||07-NOV-08
23572|Eel Creek Formation|23128|5|Briefly described|p372||Proterozoic|Age: Middle Proterozoic.||||||
23572|Eel Creek Formation|23415|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Tarcunyah Group.  Black, blue, green and grey mudstone, shale, siltstone, and thin-bedded sandstone; minor galuconitic and tuffaceous sandstone, and rhyolite tuff.||||||07-JAN-08
23572|Eel Creek Formation|23583|5|Briefly described|Map Legend|||Geological Province Officer Basin.||||||
23572|Eel Creek Formation|23585|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|||||||
23572|Eel Creek Formation|23594|5|Briefly described|p6 Fig 3|||||||||
23572|Eel Creek Formation|23757|4|Described|p15|Neoproterozoic|Neoproterozoic|Of Tarcunyah Group. Mainly multicoloured shale and siltstone (detailed lithology provided). In west, unconformably overlies De Grey Group. Unconformably overlain on northern and easterly boundaries by Callawa Formation.||||||07-JAN-08
23572|Eel Creek Formation|24025|4|Described|p16|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
23572|Eel Creek Formation|24110|5|Briefly described|Plate 1|Proterozoic|Proterozoic|Geological Province: Officer Basin||||||
23572|Eel Creek Formation|39697|4|Described|p129|||||||||
23572|Eel Creek Formation|44229|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Tarcunyah Group.  Black, blue green and grey mudstone, shale, siltstone and thin-bedded sandstone; minor glauconitic and tuffaceous sandstone, and rhyolite tuff.  geological province: Eel Creek Basin.||||||10-NOV-04
23572|Eel Creek Formation|44443|5|Briefly described|map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
23572|Eel Creek Formation|46319|4|Described|p15|Proterozoic|Paleoproterozoic|Geological Province: Pilbara Craton.||||||07-NOV-08
23572|Eel Creek Formation|50189|3|Fully described|p25-26|Neoproterozoic|Neoproterozoic|Epiclastic and sedimentary rocks. Unconformably overlies Warrawoona Group, Warrawagine Granitoid Complex, Gorge Creek and De Grey Groups; Unconformably overlain by Paterson and Callawah Formation. Max. Thickness: >500m. Geological Province: Officer Basin.||||||
23572|Eel Creek Formation|50544|4|Described|p58, p10 Fig. 5, p16 Tb. 1|Neoproterozoic|Neoproterozoic|Epiclastic/volcaniclastic rocks.  Age: 820Ma.  Unconformably overlies Warrawoona, Gorge Creek and De Grey Groups, and Muccan and Warrawagine Granitoid Complexes; unconformably overlain by Paterson and Callawa Fms.  Max. thick: >500m.  Geol.Prov: N.Carnarv||||||
23572|Eel Creek Formation|50555|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Tarcunyah Group.  Black, blue, green and grey mudstone, shale, siltstone and thin-bedded sandstone; minor glauconitic and tuffaceous sandstone, and rhyolite tuff. Age: c.800Ma.  Geological Province: Officer Basin.||||||
23572|Eel Creek Formation|60429|4|Described|p6 Fig. 3, p25-26|Neoproterozoic|Neoproterozoic|Of Tarcunyah Group. Unconformable over Warrawoona Group, Warrawaginee Granitoid Complex, Gorge Creek and De Grey Groups; unconformable over Paterson Fm. Max. thickness: >500m. Geol.prov: Pilbara Craton. Detailed lithology included. See also p8 Fig. 4.||||||07-FEB-11
23572|Eel Creek Formation|63236|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic|Of the Tarcunyah Group.  Geological Province: Officer Basin. Hematitic conglomerate.||||||17-SEP-07
23572|Eel Creek Formation|64580|4|Described|map legend||Neoproterozoic|Of Tarcunyah Group. Mudstone, shale, siltstone, and sandstone; includes dolerite sills and dykes.||||||09-DEC-08
23572|Eel Creek Formation|64688|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Tarcunyah Group. Geological province: Officer Basin. Hematitic conglomerate formed in a near-shore environment.||||||
23572|Eel Creek Formation|67202|5|Briefly described|p231, p234-235|Neoproterozoic|Neoproterozoic|||Tarcunyah Group.||Correlative of Waroongunyah Formation.|Black, grey, blue and green mudstone, shale, siltstone, and fine-grained, thin-bedded sandstone.|
23572|Eel Creek Formation|67827|6|Mentioned|p427-428|||Northern Pilbara. Appears as Eel Creek Conglomerate in Fig.16, and is mentioned as Eel Creek conglomerate on p428.||||||
23572|Eel Creek Formation|69167|4|Described|geologyp_lut.csv|Mesoproterozoic|Mesoarchean|||||Intruded by Warakurna Supersuite|Sandstone, quartz arenite, and minor siltstone; halite pseudomorphs in fine-grained sandstone. Hematite clast conglomerate and ferruginous shale; basal unit.|
23572|Eel Creek Formation|69185|4|Described|GEOL_LUT_CSV files|Neoproterozoic|Neoproterozoic|Of Officer Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 800 Ma|Unit of Tarcunyah Group.|||Mudstone, shale, siltstone, and sandstone; includes dolerite sills and dykes|
23572|Eel Creek Formation|69538|5|Briefly described|p522 Fig.5, p533, p538|Proterozoic|Proterozoic|Originally ~25 Mt detrital iron ore deposit; now largely mined out. Ore derived from M-mplH BIF-hosted bedded deposits of Nimingarra Iron Formation.||Unit in Tarcunyah Group.|||Basal BIF marine conglomerate locally contains hematite pebbles.|
23572|Eel Creek Formation|69590|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoarchean|Events: Western Australian events. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|2940-1050 Ma (inferred)|Unit of Tarcunyah Group.|||Sandstone, quartz arenite, and minor siltstone; halite pseudomorphs in fine-grained sandstone; hematite-clast conglomerate; includes ferruginous shale; basal unit.|
23572|Eel Creek Formation|70826|6|Mentioned|p10|||Age poorly constrained. May be late Mesoproterozoic. Pilbara Craton.||||||20-MAY-20
23572|Eel Creek Formation|70936|3|Fully described|p58-64,72,74-77|Mesoproterozoic|Mesoproterozoic|Geological province: Pilbara Craton. Of Wongawobbin Basin. Thickness: more than 500m thick. Occurs along NE edge of Pilbara Craton. Crops out over area of 200km2, but inferred to extend >1000km2 to the east. Associated with Stage I (1330-1260 Ma) Albany-Fraser Orogeny and 1345-1290 Ma Mount West Orogeny. Locally folded, attributed to Paterson Orogeny east of Pilbara Craton. Cut by NE-trending Kennedy Gap Fault. Depositional setting: fluvial-deltaic with basal alluvial fan conglomerates. See p62-64 for detailed sedimentological descriptions. Intruded by fine- to coarse-grained dolerite sills and dykes. Minimum age of c. 1070 Ma constrained by in situ SHRIMP U-Pb ages from dolerite (207Pb/206Pb 1064+\-14 Ma from tranquilityite, 1077+\-9 Ma from zirconolite; Rasmussen et al., 2012), and 1050+\-22 Ma of baddeleyite from a mineral separate (Wingate et al., 2012), and invalidates previous assertions of correlations to Neoproterozoic Tarcunyah Group (WIlliams, 1999, 2000). SHRIMP U-Pb ages from two tuffs at the base of the formation yields 1310+\-8 and 1318+\-7 Ma, consistent with 1327+\-7 Ma and 1300+\-22 Ma obtained from, respectively, a ferruginous sandstone and a hematite-pebble conglomerate at the base of the formation, constraining possible maximum depositional ages. Tuffs may be derived locally, based on detrital zircons of the same age in alluvial-fan conglomerates and sandstone.|Max dep age c. 1320 Ma|||Overlain by Paterson Formation and Callawa Formation.|Mudstone, siltstone and sandstone with minor volcanic rock, and local basal conglomerate with hematite clasts and thin intercalated ferruginous sandstone and shale up to 12 m thick.|
23572|Eel Creek Formation|71003|4|Described|p58-p64, p72, p74-p77|Ectasian|Ectasian|Pilbara Craton. Interpreted as part of the newly named Wongawobbin Basin. Outcrops on the northeastern edge of the Craton near Yarrie. Interpreted as part of a fluvio-deltaic succession. Preserved thickness of approximately 500m. SHRIMP dates are derived from tuff horizons at the base of this unit and are interpreted as igneous crystallisation ages. Unconformably overlies Archean metasedimentary rocks and metavolcanic sequences. Intersected by the Kennedy Gap Fault. A stratigraphic column with detailed lithology is provided on p62 (fig 4). Intruded by fine- to coarse-grained dolerite sills and dykes.|1318+/- 7 Ma; 1310 +/- 8 Ma (SHRIMP U-Pb)|||Overlain by the Paterson Formation and by the Callawa Formation.|Unmetamorphosed silciclastic sedimentary rock including mudstone, siltstone and sandstone with minor volcanic rocks.|
23572|Eel Creek Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||shale, sandstone, greensand, mudstone|
23572|Eel Creek Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoarchean||||||Mudstone, shale, siltstone, and sandstone; locally intruded by dolerite sills and dykes.|
74814|Eelya Suite|64891|5|Briefly described|p37 Fig. 2, p41, p48-9 Tb. 1|Archean|Archean|Of the Annean Supersuite. Includes Peter Well Granodiorite. Age: 2747Ma. Geological province: Murchison Domain. Biotite granodiorite with high HFSE geochemical characteristics; weakly metmorphosed. Referred to as a Granite Suite in Fig. 2.||||||05-NOV-15
74814|Eelya Suite|66195|6|Mentioned|p599 Fig.2|||In the Annean Supersuite. Granitic.||||||13-MAR-12
74814|Eelya Suite|67129|5|Briefly described|p18 Fig.19, p33 Fig.33|Archean|Archean|Murchison Domain, Youanmi Terrane. REE plot.||Annean Supersuite|||Granites.|07-SEP-17
74814|Eelya Suite|68561|5|Briefly described|GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. Medium- to coarse-grained biotite granodiorite U-Pb zircon age: 2759 +/- 2 Ma. Suite age: 2760-2735 Ma.  From geochron file 185933.1.pdf.||Annean Supersuite||Intrudes Polelle Group.||
74814|Eelya Suite|68698|5|Briefly described|p1, p4-6, p8-11, p14-16, p27-28|Neoarchean|Neoarchean|Approximate age range given as 2750-2735 Ma in Tb.1, but 2760-2735 on p8. A biotite granodiorite has a magmatic crystallisation age of 2759 +/- 2 Ma (Wingate et al., 2010). Brief geochemistry; REE plots. Contemporaneous with Cullculli Suite.|2760-2735 Ma.|Annean Supersuite.|Peter Well Granodiorite.|Intrudes Polelle Group.|Includes granitic rocks particularly enriched in HFSE.|
74814|Eelya Suite|69181|6|Mentioned|p21|||Murchison Domain, Yilgarn Craton. Some intrusions of this suite contain HFSE enrichment.||||||
74814|Eelya Suite|69583|5|Briefly described|p49, p51|Neoarchean|Neoarchean|Murchison Domain.||Annean Supersuite.|Peter Well Granodiorite.||Granitic rocks, particularly enriched in high-field-strength elements.|
74814|Eelya Suite|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean|||Annean Supersuite|Peter Well Granodiorite|||
74814|Eelya Suite|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Annean Supersuite.|Peter Well Granodiorite.|||
74814|Eelya Suite|70020|5|Briefly described|p113,118,120,130|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton. HFSE-enriched granitic rocks display similar geochemical characteristics to VHMS-associated felsic rocks of the Greensleeves Formation.||Unit of Annean Supersuite.|Includes Peter Well biotite granite, Eelya granitoid, Peter Well monzogranite, Peter Well granodiorite and  Keygo granophyric granodiorite.|Overlain by Austin Downs Suite. Underlain by Cullculli Suite.||
74814|Eelya Suite|70030|5|Briefly described|p190,192,205,208|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton. High-Field Strength Element (HFSE) igneous suite characterised by relatively flat-REE profiles, as well as low Zr/Y, Th/Yb and La/Yb. Coeval with Polelle Group volcanism, and formation of the Hollandaire VMS deposit in the lower Greensleeves Formation.|ca. 2760 Ma|Unit of Annean Supersuite.|Includes Peter Well Granodiorite.|||
74814|Eelya Suite|70139|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|2759-2747 Ma.|Annean Supersuite.|||Biotite granodiorite, weakly metamorphosed.|
74814|Eelya Suite|70796|5|Briefly described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_interpgeop_lut.csv., 500k_interpgeop_lut.csv, 185933.1.pdf, Reedy100_2543_stratig.pdf.|ca 2765 to 2735 Ma (inferred)|Annean Supersuite||Intrudes the Polelle Group.|Biotite granodiorite; weakly metamorphosed|
74814|Eelya Suite|70830|5|Briefly described|p9|||Murchison Domain.||Annean Supersuite||||
74814|Eelya Suite|71168|5|Briefly described|p7, p60|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Hosts HFSE-enriched intrusive rocks. |c. 2770-2740 Ma|Annean Supersuite|Includes the Peter Well Granodiorite, Eelya granite and the Keygo granophyric granodiorite.||Granitic rocks.|
74814|Eelya Suite|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). Sample GSWA 185933 (bt granodiorite) yielded a weighted mean 207Pb/206Pb date of 2759+\-2 Ma, interpreted as the igneous crystallization age of the granodiorite. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.|2765-2735 Ma|Unit of Annean Supersuite.||Intrudes into Poelle Group.|Biotite granodiorite; weakly metamorphosed|
25891|Egan Formation|22496|6|Mentioned|p11||Neoproterozoic|Louisa Downs Group.||||||14-APR-08
25891|Egan Formation|22764|4|Described|Table1, p6||Adelaidean|Of Louisa Downs Group||||||01-FEB-10
25891|Egan Formation|22899|5|Briefly described|86|||||||||
25891|Egan Formation|22901|6|Mentioned|78|||||||||
25891|Egan Formation|23314|5|Briefly described|331 Fig.2|||||||||
25891|Egan Formation|23383|4|Described|p21, p18 Tb.2|Neoproterozoic|Neoproterozoic|Basal unit of Louisa Downs Group. Tillite, coarse-grained quartz sandstone and arkose.  Disconformably overlain by Yurabi Formation; unconformably overlies King Leopold Sandstone. Max. thickness: 40 m.  Geological Province: Louisa Basin.||||||25-JAN-05
25891|Egan Formation|23599|4|Described|p18|Neoproterozoic|Neoproterozoic|Of Louisa Downs Group. Overlain by Yurabi Formation. Underlain by Mount Christine Granitoid. Geological Province: Louisa Basin. Max. thickness: 40 m.||||||20-DEC-07
25891|Egan Formation|23601|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Louisa Downs Group. Tillite, arkose, dolomite, limestone, sandstone, siltstone and shale.||||||25-JAN-05
25891|Egan Formation|23621|5|Briefly described|p34|||Of Louisa Downs Group.||||||
25891|Egan Formation|23806|3|Fully described|p1121|Neoproterozoic|Neoproterozoic|Of Louisa Downs Group. Max. thickness: 80m. Can be divided into three informal units.||||||14-APR-08
25891|Egan Formation|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
25891|Egan Formation|32660|5|Briefly described|Table 6|||||||||
25891|Egan Formation|32728|6|Mentioned|Table 7|||See also Fig.16||||||
25891|Egan Formation|35120|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
25891|Egan Formation|36048|6|Mentioned|p377|||||||||
25891|Egan Formation|36551|6|Mentioned|Table 10|||||||||
25891|Egan Formation|36888|4|Described|p214|||||||||
25891|Egan Formation|36898|5|Briefly described|Table IV|||See also Fig.2B & P181.||||||
25891|Egan Formation|37462|5|Briefly described|p293|||||||||
25891|Egan Formation|37927|4|Described|p504|||||||||
25891|Egan Formation|38157|6|Mentioned|Table X|||||||||
25891|Egan Formation|38243|6|Mentioned|Fig.2|||||||||
25891|Egan Formation|38988|6|Mentioned|Fig.4|||||||||
25891|Egan Formation|41405|5|Briefly described|p206|||||||||
25891|Egan Formation|41429|6|Mentioned|p247|||||||||
25891|Egan Formation|44140|4|Described|p300, p301 fig 4-7, p303 Tb.4-2|Neoproterozoic|Neoproterozoic|Of Mount Ramsay area. Laterally persistent. Correlated with Marinoan glaciation (670 Ma); coeval with Walsh and Moonlight Valley Tillites.||Louisa Downs Group||Overlies Kuniandi Group unconformably. Is overlain by Yurabi Formation.|Tillite, conglomerate and quartz sandstone; upper part dolomite and limestone. Capped with a persistent pink-dolomitic unit.|07-MAR-18
25891|Egan Formation|44231|5|Briefly described|Map Legend|Neoproterozoic III|Neoproterozoic III|Of the Louisa Downs Group. Tillite, arkose, dolomite, limestone, sandstone, siltstone ans shale. geological Province: Louisa Basin.||||||26-MAY-05
25891|Egan Formation|44397|14|Not recorded|p.20,22, Table 3||Adelaidean|Louisa Downs Group. Defn. on Tech.File E/52-9.||||||
25891|Egan Formation|44398|14|Not recorded|map legend||Adelaidean|||||||
25891|Egan Formation|44693|5|Briefly described|Map Legend||Proterozoic|||||||
25891|Egan Formation|44694|5|Briefly described|Map Legend||Proterozoic|||||||
25891|Egan Formation|45047|4|Described|p36|||Louisa Downs Group.||||||14-APR-08
25891|Egan Formation|45155|6|Mentioned|p28|||Correlation||||||
25891|Egan Formation|48927|2|Defined|p20|Adelaidean|Adelaidean|||||||
25891|Egan Formation|61574|5|Briefly described|p690|Neoproterozoic III|Neoproterozoic III|Of the Louisa Downs Group. Together with the Yurabi Formation, unconformably overlies (locally) the Crowhurst Group.||||||10-MAY-06
25891|Egan Formation|61732|5|Briefly described|p30, p65|||Deposited in association with the Egan glaciation (555-560Ma)of the central Kimberley area. Middle Ediacaran in age. See also p110.||||||07-FEB-11
25891|Egan Formation|63458|5|Briefly described|p871-874, p877 Tb.1, p882-884, p889-900.|Ediacaran|Ediacaran|c.80 m thick. Carbonate units include patch reefs, sandy shoals and lagoonal muds that developed in a shelf setting; interrupted by ice sheet advance and deposition of lodgement till and meltwater outwash. Isotopic and elemental composition of carbonate unit given.||Basal unit in Louisa Downs Group.||Is overlain by Yurabi Formation.|Mostly dolomitic; contains a metre- to decimetre-scale diamictite unit between lower and upper carbonate units.|
25891|Egan Formation|63762|5|Briefly described|p19|||Of Louisa Downs Group. Displays well-preserved glacially striated pavements. Includes an impressive stromatolite reef above the diamictite, as well as laminated sandy dolostone and oolitic and intraclastic reef facies.||||||07-FEB-11
25891|Egan Formation|66569|6|Mentioned|p863,|||Glaciogenic.||||||
25891|Egan Formation|67484|5|Briefly described|p294, p295 Fig.2, p296|||Mount Ramsay area, West Kimberley. Contains domical form and Tungussia julia (Grey and Corkeron, 1998) fossils.||Of the Louisa Downs Group.||Is overlain by Yurabi Formation. Correlated with the Boonall Dolomite, Julie Formation, Wonoka Formation.||
25891|Egan Formation|67620|5|Briefly described|p2, 5, 7-8|Neoproterozoic|Neoproterozoic|Mount Ramsay area, Kimberley region. Type section is at a road cutting of the Great Northern Highway in the Egan Range. Represents the Ediacaran/Gaskiers glaciation. Photographs.||Louisa Downs Group.||Overlies Mount Bertram Sandstone (Kuniandi Group). Is overlain conformably by Yurabi Formation. Is correlated with Boonall Dolomite, Julie and Wonoka Formations.|Has a cap dolostone at the top.|
25891|Egan Formation|68138|5|Briefly described|p153-154, 156-158, 160|Neoproterozoic|Neoproterozoic|Mount Ramsay area. Correlations based on common stromatolite (Tungussia sp.) occurrences. The type section is at Mount Ramsay. Photographs, photomicrographs.||Louisa Downs Group.||Correlated with Boonall Dolomite; also with Wonoka Formation (SA).|Lower ~4m purple-reddish cap dolostones below a 1.2m thick distinct yellow dolostone bed. Cap dolostones are rich in fine but often deformed algal laminae and tepee structures, implying shallow depositional environment.|
25891|Egan Formation|68244|4|Described|p659-660,662-666,669-671|Neoproterozoic|Neoproterozoic|Louisa Basin, Kimberley region. Glaciogenic unit deposited during Egan Glaciation. Correlation of the Egan Formation with the Centralian Superbasin using stromatolite biostratigraphy (Grey and Corkeron 1998), litho- and chemo-stratigraphy (Corkeron and George 2001; Corkeron 2007a) suggests that it records the youngest Proterozoic glaciation in Australia. See p665-666 for detailed lithology and depositional environment. Correlative to Boonall Dolomite. ContainsTungussia julia, a stromatolite biostratigraphic marker that correlates Julie Fm (Central Australia) and Bonney Sandstone (SA) to Egan Formation. Carbonate units likely deposited in a shallow, moderate- to high-energy, warm water environment.||Unit of Louisa Downs Group.||Basal glaciogenic unit of Louisa Downs Gp. Overlain by Yurabi Fm. Underlain by Mt Bertram Sst, unconformably by Kimberley, Crowhurst, Glidden Gps, Colombo Sst, Lamboo Cplx.|Dolomite and limestone with interbedded siliciclastic diamictite, conglomerate and sandstone.|
25891|Egan Formation|68271|5|Briefly described|p697|||Kimberley region. Glaciogenic succession potentially coeval with Cottons Breccia (Grassy Group; King Island TAS).||||||
25891|Egan Formation|68274|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|||||||
25891|Egan Formation|68275|6|Mentioned|p60|||Kimberley region. Here, positive values of 13C isotopes in coupled carbonates characterize carbonates overlying this Formation (challenging the suggestion that 13C isotope anomalies and glaciation are time-related).||||||
25891|Egan Formation|68276|6|Mentioned|p73|Ediacaran|Ediacaran|Kimberley region. The diamictite represents a short-lived glacial incursion onto a carbonate platform. The ""Formation"" is omitted.",,|||||Diamictite and overlying conglomerate are overlain by c.15m of dolostone, and an additional c.15m of interbedded quartz-arenite and silty dolostone with a distinctive stromatolite (Tungussia julia) horizon near the top.|
25891|Egan Formation|68277|5|Briefly described|p95|Neoproterozoic|Neoproterozoic|Central Kimberley region.||||Correlated with Boonall Dolomite and Julie Formation.|Glaciogenic deposits.|
25891|Egan Formation|68473|6|Mentioned|p531|||Mount Ramsay.||Duerdin Group||Equivalent to the Traine Formation, Throssell Shale and the Estaughs Formation.||
25891|Egan Formation|68733|6|Mentioned|p189 Fig.8|Ediacaran||Wolfe Basin.||||Equivalent to Julie Formation.||05-DEC-17
25891|Egan Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Cryogenian|Cryogenian|Louisa Basin||Louisa Downs Group|||Tillite, arkose, dolomite, limestone, sandstone, siltstone, and shale|31-JUL-15
25891|Egan Formation|69165|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran||||||Tillite, arkose, dolomite, limestone, sandstone, siltstone and shale.|
25891|Egan Formation|69437|5|Briefly described|p22:7|||Louisa Basin. Discussed in relation to a third Ediacaran glaciation event.|||||Glacial deposits.|12-JUL-16
25891|Egan Formation|69634|4|Described|100k_interpgeop_lut.csv|Cryogenian|Cryogenian|Geological province: Halls Creek Orogen. Of Louisa Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1.|850-635 Ma (Biostrat)|Unit of Louisa Downs Group.|||Tillite, arkose, dolomite, limestone, sandstone, siltstone, and shale|
25891|Egan Formation|70154|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran||541-635 Ma|Louisa Downs Group|||Tillite, arkose, dolomite, limestone, sandstone, siltstone, and shale|
25891|Egan Formation|71146|6|Mentioned|p21|Middle Ediacaran|Middle Ediacaran|Partially equivalent to the Boonall Dolomite. ||||||
25891|Egan Formation|71267|4|Described|GEOL_LUT_CSV files|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Louisa Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|635-541 Ma (biostrat)|Unit of Louisa Downs Group.|||Tillite: poorly sorted medium grained sandstone with conglomerate containing faceted boulders, siltstone, and in the upper part, limestone and dolomite partly replaced by chert|
25891|Egan Formation|73255|6|Mentioned|p532, p542|Ediacaran|Ediacaran|Contains the stromatolite Tungussia julia.|||||Limestone.|
23573|Egret Formation|13255|6|Mentioned|p369|Early Cretaceous|Late Jurassic|Roebuck Basin.||||Overlies Baleine Formation. Is overlain by Broome Sandstone.||
23573|Egret Formation|41732|6|Mentioned|Fig.3|||||||||
23573|Egret Formation|44143|4|Described|p.432 Table 4-19; p.449|Jurassic|Jurassic|>250m thick; sandstone and minor claystone; marginal marine. Conformably (west) and disconformably (east) overlies Baleine Formation. ||||||23-NOV-17
23573|Egret Formation|69297|6|Mentioned|p337, p352|Berriasian|Tithonian|Canning and Roebuck Basins. ||||Overlies the Baleine Formation. Overlain by the Mermaid Formation.||
23573|Egret Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Roebuck Basin.||||Overlies Eliassen Formation. Is overlain by Broome Sandstone.||
23573|Egret Formation|70065|5|Briefly described|Rowley: Fig.2; p2. Regional: Fig.4; p4|Berriasian|Berriasian|Roebuck Basin and offshore Canning Basin. Delta sands form reservoirs.||||Is enclosed by Baleine Formation.|Condensed marine mudstones.|
34215|Elang Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p216|Late Jurassic|Middle Jurassic|In figure, Fm = Formation. Geological Province: Bonaparte Basin. Broadly equivalent to the Montara beds. Also on p230.||||||
34215|Elang Formation|13267|5|Briefly described|pp273-279.|Middle Jurassic|Middle Jurassic|Poor hydrocarbon reservoir quality. Oil shows were observed. Very late stage oil input, probably from adjacent generating carbonaceous claystones. Calcite and ankerite cement deposited during Late Cretaceous via faults.||||Overlies Plover Formation.|Quartzose, very fine- to fine-grained, moderately well-sorted sandstones with interbedded siltstone and claystone. Clay content and carbonate cement in sandstones are variable but macroporosity is greatly reduced.|
34215|Elang Formation|13354|6|Mentioned|p381.|Jurassic|Jurassic|Sahul Platform.||15||||28-OCT-14
34215|Elang Formation|22663|6|Mentioned|NT97 -1-4 p3|||||||||
34215|Elang Formation|23376|4|Described|p229 Fig.2;p227-9,235,240,243|Oxfordian|Callovian|In the Bonaparte Basin.||||||15-AUG-06
34215|Elang Formation|24234|5|Briefly described|p286, p287 Fig.3|Callovian|Callovian|Overlies Plover Formation, overlain by Frigate Formation. Geological Province: Bonaparte Basin.||||||
34215|Elang Formation|24390|5|Briefly described|p3 Table 1|Middle Jurassic|Middle Jurassic|Geological Province: Bonaparte Basin||||||
34215|Elang Formation|24427|5|Briefly described|p49 Fig.2|Late Jurassic|Middle Jurassic|Geological Province: Bonaparte Basin.||||||09-MAR-05
34215|Elang Formation|60386|6|Mentioned|p300, 302|Late Jurassic|Middle Jurassic|Bonaparte Basin. Deltaic-nearshore-shelf, proximal shelf. ||||||
34215|Elang Formation|64689|5|Briefly described|p7 Fig.6 |Late Jurassic|Middle Jurassic|||||||
34215|Elang Formation|64696|6|Mentioned|p125, 127 Fig.2, p128, p131-132  |Late Jurassic|Middle Jurassic|See also p136, p138. Reservoir unit, c.150 m thick. Referred to as Elang/Laminaria Formation in the Joint Petroleum Development Area. Geophysical properties detailed in Fig.10.||||Overlies Plover Formation gradationally.|Sheet-like deposition of sand-prone marine and deltaic facies (sandstones, siltstones and mudstones).|
34215|Elang Formation|68135|6|Mentioned|p61, p62|||Northern Bonaparte Basin. Sedimentary sequences and fossils described.||||||14-SEP-17
34215|Elang Formation|69452|5|Briefly described|p36:8, 15, 21-22|Oxfordian|Callovian|Petrel Sub-basin, Bonaparte Basin. Thickness up to ?50m.||Flamingo Group.||Is overlain by Frigate Shale. Equivalent to Laminaria and Montara Formations.|Retrogradational deltaic sandstone deposited as a result of a widespread marine transgression.|12-JUL-16
34215|Elang Formation|69653|5|Briefly described|p1, 6, 8, 10, p13 Fig.2.4, p17-18, 76|Late Jurassic|Middle Jurassic|Petrel Sub-basin. Suitable for CO2 storage; sealed by Frigate Shale. Delta-plain - shoreface deposits. Schematic (gamma ray) well sections. Composite well diagram. Photomicrographs. See also p26-27, 30, 37, 39, 41-43, 45-48, 50, 53, 59, 63-64.||Flamingo Group.||Overlies Plover Formation. Is overlain disconformably by Frigate Shale.|Mudstone; siltstone/fine-grained sandstone; medium- to coarse-grained sandstone. Facies described in detail.|
34215|Elang Formation|69673|6|Mentioned|p173|||||Flamingo Group||||
34215|Elang Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Bonaparte Basin.||||Overlies Plover Formation.||
34215|Elang Formation|70061|5|Briefly described|Petrel Sub-basin Fig.2|Late Jurassic|Middle Jurassic|See also Regional geology: Figs.6-7, p6, p7, p10, p12, p14, p18-19. Sahul: Fig.2, p1-2. Bonaparte Basin; commercial petroleum and gas reservoir. Appears also as Elang (Laminaria) Formation. Source rock in Sahul Syncline.||Flamingo Group.||Overlies Plover Formation. Is overlain by Lower Frigate Shale.|Retrogradational deltaic (shoreface/barrier bar) sandstones.|12-JUL-16
26535|Elder Subgroup|14019|4|Described|p21|||Lower portion of the Goose Hole Group.  Overlies the Negri Subgroup (Goose Hole Group).   Geological Province: Ord Basin.||||||
26535|Elder Subgroup|22547|5|Briefly described|p30|||Of the Goose Hole Group. Overlain by Negri Subgroup.||||||14-NOV-06
26535|Elder Subgroup|40993|6|Mentioned|Fig.1|||||||||
26535|Elder Subgroup|41840|4|Described|p43|||Formerly "Mount Elder sandstone", In part Elder Sandstone||||||
26535|Elder Subgroup|41864|5|Briefly described|p23|||Formerly Elder Sandstone||||||
26535|Elder Subgroup|41865|6|Mentioned|Map legend|Late Cambrian|Middle Cambrian|||||||
26535|Elder Subgroup|41866|6|Mentioned|Map legend|Late Cambrian||||||||
26535|Elder Subgroup|43855|5|Briefly described|Map Legend|Boomerangian|Templetonian|||||||
26535|Elder Subgroup|44230|5|Briefly described|Map Legend||Middle Cambrian|||||||
26535|Elder Subgroup|44868|5|Briefly described|Map Legend|Boomerangian|Ordian|||||||
26535|Elder Subgroup|60419|4|Described|p1, p3 Fig.2|Late Cambrian|Middle Cambrian|Of Goose Hole Group. Conformably overlies Negri Subgroup. Max. thickness: 370 m. Geological Province: Ord Basin.||||||
26535|Elder Subgroup|60519|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Goose Hole Group. Includes: Eagle Hawk Sandstone, Overland Sandstone. Geological Province: Ord Basin.||||||03-NOV-04
26535|Elder Subgroup|60589|5|Briefly described|Map legend|Late Cambrian|Middle Cambrian|Of the Goose Hole Group.  Geological Province: Ord Basin.||||||
26535|Elder Subgroup|67860|5|Briefly described|p417, p419 Tb. 4-18, p421 fig 4-86|Late Cambrian|Middle Cambrian|95-370 m thick.||Goose Hole Group|Includes Eagle Hawk and Overland Sandstones.|Conformably overlies Negri Subgroup.|Feldspathic sandstone; minor siltstone.|
26535|Elder Subgroup|69099|5|Briefly described|GEOL_LUT_CSV files + geochron files|Furongian|Furongian|Ord Basin||Goose Hole Group|Includes Eagle Hawk Sandstone, Overland Sandstone|||
26535|Elder Subgroup|69165|6|Mentioned|100k_interpgeop_lut.csv, |Furongian|Furongian|||Goose Hole Group|Includes Eagle Hawk Sandstone, Overland Sandstone,|||
26535|Elder Subgroup|69448|4|Described|p33:1-4, 6-8|Middle Cambrian|Middle Cambrian|Ord Basin. Previously Elder Sandstone. Up to 370m thick. Lacks age-diagnostic fossils.||Goose Hole Group.|Eagle Hawk, Overland Sandstones.|Conformably and gradationally overlies Negri Subgroup. Is overlain unconformably by Mahony Group.|A sandstone-dominated succession.|12-JUL-16
26535|Elder Subgroup|69634|5|Briefly described|100k_interpgeop_lut.csv|||||Unit of Goose Hole Group.|Includes Eagle Hawk Sandstone, Overland Sandstone.|||
26535|Elder Subgroup|69673|5|Briefly described|p193, p194|||370m thick.|||Includes Eagle Hawk Sandstone, Overland Sandstone||Sandstones.|
26535|Elder Subgroup|70154|6|Mentioned|100k_interpgeop_lut.csv|Ordovician|Cambrian||485-509 Ma|Goose Hole Group|Includes Eagle Hawk Sandstone, Overland Sandstone|||
26535|Elder Subgroup|71146|5|Briefly described|p6|Cambrian|Cambrian|Ord Basin.||Goose Hole Group||Overlies the Negri Subgroup. Unconformably overlain by the Mahony Group.|Sandstone.|
26535|Elder Subgroup|71267|5|Briefly described|100k_interpgeop_lut.csv|||Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny (450-295 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma).||Unit of Goose Hole Group.|Includes Eagle Hawk Sandstone, Overland Sandstone.|||
26535|Elder Subgroup|71800|5|Briefly described|p25-p26|Late Cambrian|Middle Cambrian|Ord Basin.||Goose Hole Group|Includes the Eagle Hawk Sandstone and the Overland Sandstone.|Overlies the Negri Subgroup.||
83643|Elephant Rocks basaltic dyke|73480|5|Briefly described|p212||Tonian|N-NE trending, shallowly dipping sill. Age based on one grain. See also Elephant Rocks dyke. Intrudes a biotite metagranite with a minimum cooling age of ca 970 Ma.|942+/-11 Ma U-Pb zircon maximum age, (<ca 250 Ma?)||||Microporphyritic ophitic basalt dyke, unmetamorphosed.|
39603|Eley Monzogranite|24531|5|Briefly described|p29, p31|Archean|Archean|Of the Shaw Granitoid Complex. A weakly to moderately foliated, K-feldspar-porphyritic biotite monzogranite. See also p8-9 Fig. 3.||||||15-APR-13
39603|Eley Monzogranite|24532|5|Briefly described|Map legend|Archean|Archean|Of the Shaw Granitoid Complex.  Age: >2929 Ma.||||||15-APR-13
39603|Eley Monzogranite|50381|5|Briefly described|Map Legend|Archean|Archean|Of Shaw Granitoid Complex. Geological Province: Pilbara Craton.||||||07-NOV-08
39603|Eley Monzogranite|50427|5|Briefly described|p187 Fig.8|Archean|Archean|Age: 2930 Ma. Of Shaw Granitoid Complex.||||||07-NOV-08
39603|Eley Monzogranite|63441|5|Briefly described|p11 Tb. 2|Archean|Archean|Of Sisters Supersuite. Supersedes Eley Adamellite. Geological province: Pilbara Craton. ??Also included in Split Rock Supersuite in Table 2. (??)||||||07-FEB-11
39603|Eley Monzogranite|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Unit in Sisters Supersuite. K-feldspar-porphyritic biotite monzogranite; weakly foliated.||||||
39603|Eley Monzogranite|68282|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|2927-2908 Ma|Of the Sisters Supersuite|||K-feldspar-porphyritic biotite monzogranite; weakly foliated.|
39603|Eley Monzogranite|69012|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|c. 2928 Ma|Of the Sisters Supersuite.|||K-feldspar-porphyritic biotite monzogranite; weakly foliated.|29-APR-14
39603|Eley Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Sisters Supersuite|||K-feldspar-porphyritic biotite monzogranite; weakly foliated.|
39603|Eley Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; North Pilbara Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.|2954-2919 Ma (inferred)|Unit of Sisters Supersuite.|||K-feldspar-porphyritic biotite monzogranite; weakly foliated|
39603|Eley Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
39603|Eley Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Sisters Supersuite|||Porphyritic biotite monzogranite; numerous K-feldspar phenocrysts; weakly foliated; metamorphosed.|
75545|Eliassen Formation|60379|5|Briefly described|p126 fig 3, p127, 128, p130,  p133|Oxfordian|Oxfordian|Dampier sub-basin, Carnarvon Basin. Fine-grained, low-energy offshore sedimentation.From near base of  W.spectabilis biozone to sequence boundary top near top of W.clathrata biozone.||||||
75545|Eliassen Formation|60386|6|Mentioned|p302|Oxfordian|Oxfordian|Northern Carnarvon Basin. Distal shelf/basin.||||||
75545|Eliassen Formation|67368|6|Mentioned|p209 Fig.4.|Oxfordian|Oxfordian|||||Overlies Calypso Formation. Is overlain by Dingo Formation.||
75545|Eliassen Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Northern Carnarvon Basin.||||Overlies Calypso Formation. Is overlain by Angel Formation, Egret Formation.||
75545|Eliassen Formation|70066|5|Briefly described|Dampier: Fig.2. Regional: Fig.6; p6|Oxfordian|Oxfordian|Dampier Sub-basin, Northern Carnarvon Basin. Significant petroleum reservoir.||||Overlies Calypso Formation. Is overlain by and interfingers with Dingo Claystone. Equivalent to Biggada Formation.||
30279|Eliot Range Dolomite|22496|4|Described|p10||Neoproterozoic|Previously mapped as Bungle Bungle Dolomite.  Of the Ruby Plains Group.  Geological Province:  Wolfe Basin.||||||12-AUG-04
30279|Eliot Range Dolomite|22777|5|Briefly described|Map|||Ruby Plains Group, Wolfe Basin||||||
30279|Eliot Range Dolomite|23314|4|Described|330|Cryogenian|Tonian|Of Wolfe Basin. Includes Linella avis stromatolites, of restricted Neoproterozoic age range.||||||31-JAN-14
30279|Eliot Range Dolomite|23621|2|Defined|p52 Appendix|Cryogenian|Tonian|See also page 33, 9 table 1. Type section included. Of Ruby Plains Group. Overlying unit Illjarra Sandstone. Underlying unit Mount Kinahan Sandstone. Wolfe Basin. Max. thickness: <500 m.||||||
30279|Eliot Range Dolomite|23622|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Ruby Plains Group. Geological Province: Wolfe Basin.||||||
30279|Eliot Range Dolomite|24173|4|Described|p24, p11 Tb.2|Tonian|Tonian|Of Ruby Plains Group; previously of Bungle Bungle Dolomite. Dolomitic mudstone, siltstone and sandstone. Conformably overlain by Illjara Sandstone; conformably underlain by Mount Kinahan Sandstone.  Geological Province: Wolfe Basin. Max Thickness: 300m.||||||06-APR-05
30279|Eliot Range Dolomite|43299|5|Briefly described|Map Legend||Neoproterozoic|of Duerdin Group.[Changed to Ruby Plains Group on later edition]||||||
30279|Eliot Range Dolomite|43303|5|Briefly described|Map Legend||Neoproterozoic|of Ruby Plains Group.||||||
30279|Eliot Range Dolomite|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Ruby Plains Group. Geological Province: Wolfe Creek Basin. Age: c.?800Ma. Dolomitic mudstone, siltstone and sandstone.||||||
30279|Eliot Range Dolomite|64104|6|Mentioned|p69|||Formerly Bungle Bungle Dolomite. See also references to the currently informal name, Eliot Range Formation (p63 Fig.1, p76 fig 10, p77). Source of clasts in Fargoo Formation at Palm Springs.||||||
30279|Eliot Range Dolomite|67484|6|Mentioned|p294|Neoproterozoic|Neoproterozoic|Kimberley Region. Assigned to the early to middle Neoproterozoic in age by stromatolite biostratigraphic correlation.||||Overlies Mount John Shale Member.||
30279|Eliot Range Dolomite|68244|6|Mentioned|p668-p669|||Erosion and remobilisation of carbonate leading to abundant carbonate framework clasts and high carbonate content of lower Duerdin Group glaciogenic units (Fargoo and Mountain Valley Fms; Corkeron 2008).||Unit of Ruby Plains Group.||Uppermost unit of Ruby Plains Group. Unconformably overlain by Duerdin Group/Fargoo Formation.||21-JUN-19
30279|Eliot Range Dolomite|68733|6|Mentioned|p189 Fig.8|Cryogenian|Cryogenian|Wolfe Basin.||Of the Ruby Plains Group.||Correlated with Bitter Springs Formation and Angalarri Siltstone.||05-DEC-17
30279|Eliot Range Dolomite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Cryogenian|Cryogenian|Wolfe Creek Basin||Ruby Plains Group|Includes unnamed dolomitic sandstone member.||Dolomitic mudstone, siltstone, and sandstone|31-JUL-15
30279|Eliot Range Dolomite|69165|4|Described|100k_interpgeop_lut.csv|Neoproterozoic|Neoproterozoic|||Ruby Plains Group|||Dolomitic mudstone, siltstone and sandstone.|
30279|Eliot Range Dolomite|69634|4|Described|100k_interpgeop_lut.csv|Cryogenian|Cryogenian|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1.|830-810 Ma (Inferred)|Unit of Ruby Plains Group.|||Dolomitic mudstone, siltstone, and sandstone|
30279|Eliot Range Dolomite|70154|5|Briefly described|100k_interpgeop_lut.csv|Cryogenian|Neoproterozoic||810-1000 Ma|Ruby Plains Group|||Dolomitic sandstone, mudstone and siltstone.|
30279|Eliot Range Dolomite|71267|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|830-720 Ma (inferred)|Unit of Ruby Plains Group.|||Dolomitic mudstone, siltstone and sandstone; minor dolomitic breccia and black chert; stromatolitic|
76742|Eliza Formation|68995|5|Briefly described|p7 Fig.3, p12-13, p21, p24, p27 Tb. 2|Stenian|Stenian|Best exposure occurs in the Mount Eliza-Barrow Range region. Also includes minor basalt, basaltic andesite lavas, siliciclastic conglomerates, sandstones and mudstones. Where the Mount Waugh rhyolite is absent this formation is overlain by diamictite that may be the base of the Kaarnka Group. Metamorphism briefly discussed. See also p43, p61.||Mount Palgrave Group||Overlies (or is intruded by) the Winburn Granite. Overlain by the Scamp Formation or Mount Waugh rhyolite.|Aphyric to sparsely feldspar-phyric, vitric rhyolites with local voluminous and laterally continuous units of perlitic and spherulitic rock. Also includes clast-rich, non-welded ignimbrite deposits, diamictitic deposits and autoclast breccias.|
76742|Eliza Formation|69009|5|Briefly described|Map Legend|Stenian|Stenian|Bentley Basin.|1077-1063 Ma|Of the Mount Palgrave Group.|||Comprises clast- to matrix-supported conglomerate; rhyolitic volcaniclastic sandstone; rhyolite lava flows, minor subvolcanic sills, and pyroclastic rocks.|
76742|Eliza Formation|69091|5|Briefly described|p71 Fig.4.14|||Presented as Eliza Fm in figure.||Mount Palgrave Group|||Sedimentary.|
76742|Eliza Formation|69153|5|Briefly described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen||Mount Palgrave Group|||Rhyolite lavas, amygdaloidal dacite lavas, pyroclastic rocks, volcanic siltstones; rhyolitic volcaniclastic sandstone; vesicular and amygdaloidal basalt; basaltic andesite; rhyolite breccia; conglomerate (basalt, rhyolitic lavas); minor sills|
76742|Eliza Formation|69729|6|Mentioned|p82|||Bedrock of Talbot Sub-basin.||Mount Palgrave Group.||||
76742|Eliza Formation|70095|5|Briefly described|p17,19,21|||Geological province: Musgrave Province. Of Talbot Sub-basin, Bentley Basin. See p19 Table 2 for U-Pb zircon data. See p21 Table 3 for SIMS oxygen isotope data.||Unit of Mount Palgrave Group.||Overlain by Scamp Formation. Underlain by Winburn granite or Giles Intrusions or Kunmarnara Group.||
76742|Eliza Formation|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|SHRIMP ages derived from rhyolite sample (195116.1.pdf)|1047 Ma - 1077 Ma (Inferred) 1077 Ma (SHRIMP)|Mount Palgrave Group|||Vesicular and amygdaloidal basalt, basaltic andesite and dacite. Flow banded rhyolite, rhyolitic conglomerate, autoclastic breccia and volcaniclastic sandstone. Clast-matrix supported conglomerate; pyroclastic rock.|
76742|Eliza Formation|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Sample GSWA 194800 (rhyolite) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) magmatic crystallisation age of 1070+\-6 Ma. Sample GSWA 195114 (dacite) yielded an intepreted (207Pb*/206Pb* and 238U/206Pb* concordia) magmatic crystallisation age of 1066+\-5 Ma. Sample GSWA 195115 (felsic volcaniclastic rock) yielded an intepreted (weighted mean 207Pb*/206Pb*) magmatic crystallisation age of 1070+\-10 Ma. Sample GSWA 195116 (dacite) yielded an intepreted (weighted mean 207Pb*/206Pb*) magmatic crystallisation age of 1077+\-8 Ma. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 500k_interpgeop_lut.csv.|1077-1047 Ma (inferred)|Unit of Mount Palgrave Group.||Lowermost stratigraphic unit of Mount Palgrave Group. Overlain by Scamp Formation.|Vesicular and amygdaloidal basalt and basaltic andesite, mmygdaloidal dacite lavas and subvolcanic sills, autoclastic rhyolite breccia, flow banded rhyolite as lava flows, rhyolitic volcaniclastic sandstone and conglomerate.|
76742|Eliza Formation|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Sample GSWA 194800 (rhyolite) yielded a concordia age of 1070+\-6 MA, interpreted as mean magmatic crystallisation age of the rhyolite. Sample GSWA 195114 (dacite) yielded a concordia age of 1068+\-5 Ma, interpreted as mean magmatic crystallisation age of the dacite. Sample GSWA 195115 (felsic volcaniclastic) yielded a weighted mean 207Pb/206Pb age of 1070+\-10 Ma, interpreted as mean magmatic crystallisation age of the felsic volcaniclastic. Sample GSWA 195116 (dacite) yielded a weighted mean 207Pb/206Pb age of 1077+\-8 Ma, interpreted as mean magmatic crystallisation age of the dacite. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv.|1077-1047 Ma (inferred)|Unit of Mount Palgrave Group.||Lowermost unit of Mount Palgrave Group. Overlain by Smap Formation.|Dacite lavas and subvolcanic sills: amygdaloidal, feldspar-phyric; conglomerate with basalt clasts; rhyolite lava flows; flow-banded with subvolcanic sills; rhyolitic conglomerate and volcaniclastic sandstone; vesicular and amydaloidal basalt.|
76742|Eliza Formation|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1076+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite, dacite, felsic volcaniclastic rock.|
76742|Eliza Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|Max age 1077+/-6 Ma, Min ~1047 Ma.|Mount Palgrave Group|||Rhyolite lava flows, subvolcanic sills, and pyroclastic rocks; locally interlayered with volcanic sandstone and siltstone, and minor basalt.|
76742|Eliza Formation|72443|6|Mentioned|p738, p742||||1067 +/- 10 Ma to 1062+/- 8 Ma (SHRIMP U-Pb)|Mount Palgrave Group||||
68738|Elizabeth Hill Supersuite|63441|5|Briefly described|p36, p10 Tb. 2|Archean|Archean|Includes Cliff Pool Tonalite (in Cherratta Granitic Complex, WPS) and Cockeraga Leucogranite (in Yule Granitic Complex, EPT). Age: c. 3070Ma. Geological province: East Pilbara Terrane+West Pilbara Superterrane/Pilbara Craton. See also p32 Fig. 11.||||||07-FEB-11
68738|Elizabeth Hill Supersuite|63538|6|Mentioned|p6 Fig. 3|Archean|Archean|Geological Province: Pilbara Craton.||||||19-APR-13
68738|Elizabeth Hill Supersuite|64174|5|Briefly described|Map legend|Archean|Archean|Includes Cliff Pool Tonalite. Age: c.3068Ma. Geological province: Pilbara Craton.||||||07-NOV-08
68738|Elizabeth Hill Supersuite|64580|6|Mentioned|map legend|||||||||
68738|Elizabeth Hill Supersuite|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Pilbara Craton. Includes Cockeraga Leucogranite, as well as mapped but unnamed units of xenolith-rich leucogranite, tonalite and syenogranite.||||||
68738|Elizabeth Hill Supersuite|66217|6|Mentioned|p9, p38.|||West Pilbara Superterrane. Intruded during collision with East Pilbara Terrane at 3.07-3.05 Ga (the Prinsep Orogeny).||||||
68738|Elizabeth Hill Supersuite|67201|4|Described|p7, p11, p13, p15, p19, p24, p26|||Intrudes both West Pilbara Superterrane and western part of East Pilbara Terrane, and is not part of either major tectonic unit. Granitic magmatism intruded Sholl Terrane during collision with Karratha Terrane at 3070 Ma (Princep Orogeny). |c. 3070 Ma||Cliff Pool Tonalite|Intruded Whundo Group and Railway Supersuite.|Granitic magmatism.|22-NOV-16
68738|Elizabeth Hill Supersuite|68035|5|Briefly described|p289, p286 Fig 3, p290 Fig 5|Mesoarchean|Mesoarchean|West Pilbara Superterrane. Spelt Elizabeth Hills Supersuite p289.|3070 - 3060 Ma|||Intrudes Sholl and East Pilbara Terranes.|Tonalite and granodiorite.|
68738|Elizabeth Hill Supersuite|68280|6|Mentioned|p3|Mesoarchean|Mesoarchean||3070-3060 Ma|||||
68738|Elizabeth Hill Supersuite|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton. Mapped as 2 unnamed facies.|||||Interleaved banded and gneissic metagranodiorite, seriate to porphyritic monzogranite, and pegmatite; locally includes granitic dykes or abundant greenstone xenoliths.|30-APR-14
68738|Elizabeth Hill Supersuite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean||||Includes Cockeraga Leucogranite||Interleaved banded and gneissic metagranodiorite, seriate to porphyritic metamonzogranite, monzogranite, and pegmatite. Leucogranite; medium-coarse grained with abundant pegmatite and granitic gneiss xenoliths.Hornblende-biotite tonalite.|
68738|Elizabeth Hill Supersuite|69185|5|Briefly described|500k_geologyp08_lut.csv|||Geological Province: Pilbara Craton.|||Includes Cliff Pool Tonalite.|||
68738|Elizabeth Hill Supersuite|69301|4|Described|p5 Fig.3, p12|||Pilbara Craton. West Pilbara Superterrane.|3.07 Ga||||Granitic rocks.|
68738|Elizabeth Hill Supersuite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Prinsep Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.|3068-3066 Ma (inferred)||Includes Cockeraga Leucogranite.||Interleaved banded and gneissic metagranodiorite, seriate to porphyritic (meta)monzogranite, and pegmatite; includes local granitic dykes, leucogranite, hornblende-biotite tonalite, local greenstone and granitic gneiss xenoliths.|
68738|Elizabeth Hill Supersuite|70022|6|Mentioned|p115|||Pilbara Craton.||||||
68738|Elizabeth Hill Supersuite|70775|5|Briefly described|p5, p8 fig 5, p9|Mesoarchean|Mesoarchean|Associated with the Prinsep Orogeny. See also p13, p16, p19, p25 tbl 4, p37-p38, p44 fig 27, p47, p53, p66, p81.|c. 3068-3066 Ma||Includes the Cliff Pool Tonalite.|||
68738|Elizabeth Hill Supersuite|70826|6|Mentioned|p8|Mesoarchean|Mesoarchean|||||||
68738|Elizabeth Hill Supersuite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite, monzogranite, tonalite, granite|
68738|Elizabeth Hill Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||Max age 3068+/-4 Ma, min 3066+/-4 Ma||Includes Cockeraga Leucogranite, Cliff Pool Tonalite, and an unnamed unit.||Tonalite to syenogranite; local greenstone xenoliths; metamorphosed, with minor orthogneiss. Leucogranite; medium to coarse grained; abundant pegmatite and local greenstone and granitic gneiss xenoliths.|
68738|Elizabeth Hill Supersuite|72251|6|Mentioned|p54|||Geological province: East Pilbara Terrane and West Pilbara Superterrane, Pilbara Craton.||||||
68738|Elizabeth Hill Supersuite|72668|5|Briefly described|p4,p10, p12-13, p16, p20-21, p28|||West Pilbara Superterrane. Biotite tonalite is in the eastern part of the Cherratta Granitic Complex and gneissic granodiorite to monzogranite is interpreted as part of the Caines Well Granitic Complex.  Indications [xenocrystic zircons?] imply derivation from recycling of mafic to felsic crust. Shown as Elizabeth Hill Suite p13.|c. 3080-3060 Ma||||Biotite tonalite and possibly gneissic granodiorite to monzogranite.|13-JAN-22
68738|Elizabeth Hill Supersuite|73598|6|Mentioned|p1212|Mesoarchean|Mesoarchean|East Pilbara Terrane.||||||
36899|Ellawarrina Monzogranite|23598|2|Defined|p19 Appendix 2||Archean|Age: younger than c.3015 Ma. See also page 11. Type Locality 21o30'00"E, 117o58'10"S. Lithology: Biotite-bearing monzogranite.||||||07-NOV-08
36899|Ellawarrina Monzogranite|50370|5|Briefly described|Map Legend|Archean|Archean|Of Yule Granitoid Complex. Geological Province: Pilbara Craton||||||07-NOV-08
36899|Ellawarrina Monzogranite|63372|4|Described|Map Legend|Archean|Archean|Of the Yule Granitoid Complex. Geological Province: East Pilbara Granite-Greenstone Terrane. Age: 3165Ma. Biotite-bearing monzogranite; metamorphosed.||||||07-NOV-08
36899|Ellawarrina Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
24949|Ellendale 16 Lamproite|41158|6|Mentioned|Table 39|||||||||
39349|Ellington Granite|24091|5|Briefly described|p84|Archean|Archean|Age: 2662+/-3Ma (Pb/Pb). Geological Province: Yilgarn Craton.||||||07-NOV-08
68859|Elma Conglomerate|44231|5|Briefly described|Map Legend|Famennian|Frasnian|Boulder, cobble and pebble conglomerate; poorly exposed. Interbedded locally with Pillara Limestone and Nullara Limestone.||||||
68859|Elma Conglomerate|64580|6|Mentioned|map legend|||Frasnian and Famennian conglomerates associated with Devonian reef complexes.||||||15-DEC-08
68859|Elma Conglomerate|66127|3|Fully described|p69, pp134-139, p294, Plates 3, 7. |Early Famennian|Middle Frasnian|Formerly Mount Elma Conglomerate of Guppy et al. (1958); changed to Elma Conglomerate by Tyler et al. (1998) and this study. Type locality in a gully on NE side of Mount Elma. Deposited in front of the scarp of the Mount Elma (normal) Fault, active during the Famennian. Estimated thickness exceeds 1000 m.|c.381 - 374 Ma.|||Interfingers with Pillara and Nullara Limestones.|Quartzite-dominated cobble to boulder conglomerate; minor coarse-grained arkosic sandstone; alluvial-fan, fan-delta and submarine-fan deposits.|
68859|Elma Conglomerate|69099|5|Briefly described|500k_geologyp08_lut.csv|Famennian|Frasnian|Frasnian and Famennian conglomerates associated with Devonian reef complexes|||||Conglomerate and sandstone.|31-JUL-15
68859|Elma Conglomerate|69165|6|Mentioned|500k_geologyp08_lut.csv|Famennian|Frasnian|||||||
68859|Elma Conglomerate|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Platform and basinal boulder, cobble and pebble conglomerate; poorly exposed|
23577|Elsa Sandstone Member|40837|6|Mentioned|p260|||||||||
23577|Elsa Sandstone Member|43599|6|Mentioned|p248|||||||||
23577|Elsa Sandstone Member|43666|6|Mentioned|p21|Eifelian|Emsian|||||||
23577|Elsa Sandstone Member|64643|5|Briefly described|p3 Fig. 2|Wenlock|Llandovery|Of Worral Formation?||||||
23577|Elsa Sandstone Member|65301|5|Briefly described|p3||Silurian|Of the Worral Formation. Geological province: Canning Basin. A porous unit. ||||||
23577|Elsa Sandstone Member|65449|3|Fully described|p1, p5-6, p8-9, p29, p31-33, p38, p51-52|Wenlock|Llandovery|See also Plates 1-4, 9-11. Lehmann (1984), after Elsa Bore. Type section is the interval 596-577m in Barbwire 1. The fully cored interval 503.95-480.13m in Acacia 1 is here nominated as a reference section. From 10m to 58m thick. Deposited under clastic shoreline to mainly eolian conditions. Contains porous reservoir sands. Where Dodonea Member is absent, the term Elsa Sandstone Member is applied to the entire lower sandy part of the parent Formation.  Age inferred from relationship with Dodonea Member. Also appears as Elsa Sandstone on p51-52.||Worral Formation.||Overlies and intertongues with Dodonea Member. Is overlain by Waldecks Member.|White, pale grey or pale brown, well-sorted, porous, dominantly quartzose sandstone, typically fine- to medium-grained but locally including coarse and granular beds; locally massive or with interbeds of mudstone and minor carbonate.|
23577|Elsa Sandstone Member|68007|4|Described|p10-12, Plate 1|Silurian|Silurian|Kidson Sub-basin. 44.5m thick in Patience 2 well.||Basal Worral Formation.||Gradationally overlies Carribuddy Group.|Light pinkish grey to light grey and white, very fine- to fine-grained sandstone, interbedded with red-brown and minor greenish-grey siltstone and claystone. The sandstone and siltstone are locally dolomitic.|
23577|Elsa Sandstone Member|73117|6|Mentioned|p129|||||||||
73382|Elsie Creek Tonalite|63417|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite.  Age: 3299-3290Ma. Geological Province: Pilbara Craton. Metamorphosed, folaited to gneissic, biotite tonalite and granodiorite; minor monzogranite.||||||07-NOV-08
73382|Elsie Creek Tonalite|63441|5|Briefly described|p8 Tb. 2|Archean|Archean|Of Emu Pool Supersuite. Ages: from 3292+/-4Ma to 3290+/-4Ma. Geological province: Pilbara Craton.||||||07-FEB-11
73382|Elsie Creek Tonalite|65724|5|Briefly described|map legend|Paleoarchaean|Paleoarchaean|Of Emu Pool Supersuite. Under Hardey and Kylena Fms; intrudes Cleland Supersuite and Euro Basalt. Biotite tonalite and granodiorite; monzogranite. Age: 3299-3290 Ma (geochron. DR Nelson 2004 and in prep). Geol.Prov: East Pilbara Granite-Greenstone Terrane||||||
73382|Elsie Creek Tonalite|65825|6|Mentioned|p32.|||Appendix 2 indicates that these rocks used to be included, un-named, within the Yilgalong Granitic Complex, and are now part of the Emu Pool Supersuite, according to the GSWA databases.||Unit in Emu Pool Supersuite.||||
73382|Elsie Creek Tonalite|65829|2|Defined|p7 Fig.3, p8, pp10-12, p32, p43. |Paleoarchean|Paleoarchean|New name. Named after a tributary of the Nullagine River. Makes up almost all the Yilgalong Granitic Complex in the map area. Type areas include gorges on south bank of Elsie Creek. Is strongly deformed; intensity increases towards the greenstone belts. Intrudes Euro Basalt 3299 - 3290 Ma.|3291 +/- 4 Ma (Nelson 2005b,c).|Unit in Emu Pool Supersuite.||Intrudes Euro Basalt. Is intruded by Cleland Supersuite. Is overlain unconformably by Fortescue Group.|Gneissic to foliated, fine- to medium-grained biotite tonalite and granodiorite, minor monzogranite, tonalite gneiss; protomylonitic at the margin with Mount Elsie greenstone belt.|
73382|Elsie Creek Tonalite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Emu Pool Supersuite|||Metatonalite and metagranodiorite; minor metamonzogranite; local sills of monzogranite and orthogneiss xenoliths; strongly foliated to gneissic|
73382|Elsie Creek Tonalite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv.|3325-3277 Ma (inferred)|Unit of Emu Pool Supersuite.|||Biotite (meta)tonalite and metagranodiorite, sills of monzogranite and orthogneiss xenoliths, numerous mafic and ultramafic xenoliths.|
73382|Elsie Creek Tonalite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||tonalite, granodiorite, monzogranite|
73382|Elsie Creek Tonalite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||Max age 3292+/-4 Ma, min 3277+/-4 Ma.|Emu Pool Supersuite|||Metatonalite and metagranodiorite; local sills of monzogranite and orthogneiss xenoilths; strongly foliated to gneissic.|
25894|Emanuel Formation|7433|6|Mentioned|p25 Fig.2. |||Canning Basin.||||||
25894|Emanuel Formation|13995|5|Briefly described|p77, p79, p82-83, p86, p89, p99-100|Early Ordovician|Early Ordovician|Canning Basin. Gastropod species listed. Appears also as Emanuel Creek Formation in p77. Contains a diverse (25 species) fauna of nautiloids: all species are endemic to Australia. Trilobite assemblages; one resembles Florentine Valley Formation in Tasmania. Includes a Cheirocrinus echinoderm. Conodont fauna have some resemblance to those in Hensleigh Siltstone (NSW). Biogeographical links discussed.||||Is overlain by Gap Creek Formation.||
25894|Emanuel Formation|14228|5|Briefly described|p6 fig3|Early Ordovician|Early Ordovician|North Canning Basin.||||Overlies Kunian Sandstone. Overlain by Gap Creek Formation.||05-OCT-16
25894|Emanuel Formation|22646|6|Mentioned|p 106|Early Ordovician|Early Ordovician|Canning Basin||||||
25894|Emanuel Formation|22650|5|Briefly described|p 160|Ordovician|Ordovician|Province - Canning Basin.||||||
25894|Emanuel Formation|22741|5|Briefly described|P21, Table3 P18||Early Ordovician|||||||
25894|Emanuel Formation|22767|6|Mentioned|P11|||Correlates with the Nambeet Formation||||||
25894|Emanuel Formation|23213|5|Briefly described|p11|Bendigonian|Lancefieldian|Age: Late Lancefieldian to Middle Bendigonian. Fossil assemblage resembles the Hensleigh Siltstone conodont assemblage.||||||
25894|Emanuel Formation|23360|5|Briefly described|846 Fig.1|Ordovician|Ordovician|||||||
25894|Emanuel Formation|23373|6|Mentioned|p318||Early Ordovician|Of Canning Basin.||||||10-NOV-08
25894|Emanuel Formation|23847|5|Briefly described|p297 Fig. 1|Ordovician|Ordovician|Geological Province: Canning Basin.||||||
25894|Emanuel Formation|24061|5|Briefly described|p175|Early Ordovician|Early Ordovician|Geological Province:  Canning Basin.||||||
25894|Emanuel Formation|30110|6|Mentioned|p81|||||||||
25894|Emanuel Formation|30983|4|Described|p74|||||||||
25894|Emanuel Formation|31572|6|Mentioned|p22|||L.Ordovician. Correlation chart||||||
25894|Emanuel Formation|31706|6|Mentioned|p637|||Ordovician correlation chart||||||
25894|Emanuel Formation|32648|6|Mentioned|p32|||Camb. - Ord.||||||
25894|Emanuel Formation|33738|6|Mentioned|p44|||||||||
25894|Emanuel Formation|34999|6|Mentioned|p124|||||||||
25894|Emanuel Formation|35119|4|Described|p460|||Mentioned P455.||||||
25894|Emanuel Formation|36225|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
25894|Emanuel Formation|36257|6|Mentioned|Table 2.1|||||||||
25894|Emanuel Formation|36890|3|Fully described|p322|||Formerly Emanuel Limestone.||||||10-NOV-08
25894|Emanuel Formation|38878|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
25894|Emanuel Formation|40127|6|Mentioned|p8|||||||||
25894|Emanuel Formation|40136|5|Briefly described|p24|||||||||
25894|Emanuel Formation|41055|6|Mentioned|p46|||||||||
25894|Emanuel Formation|41215|6|Mentioned|Fig.5|||||||||
25894|Emanuel Formation|41730|6|Mentioned|Fig.3|||||||||
25894|Emanuel Formation|41854|6|Mentioned|p94|||||||||
25894|Emanuel Formation|42080|6|Mentioned|p281|||||||||
25894|Emanuel Formation|42347|6|Mentioned|Fig.2 P1020|||||||||
25894|Emanuel Formation|42880|5|Briefly described|Fig.2,p1020|||||||||
25894|Emanuel Formation|43656|6|Mentioned|Fig.2,p8|Arenigian|Tremadocian|||||||
25894|Emanuel Formation|43666|6|Mentioned|p49,Table 2|Arenigian|Tremadocian|||||||
25894|Emanuel Formation|43803|1|Redefined|p65,68||Arenig|||||||
25894|Emanuel Formation|43808|5|Briefly described|p298|||||||||
25894|Emanuel Formation|43809|6|Mentioned|p215|||||||||
25894|Emanuel Formation|44143|4|Described|p.441 Table 4-19|Ordovician|Ordovician|Unit in Prices Creek Group. Up to 746m thick; limestone, shale, dolomite & sandstone; shallow marine. Passes laterally into William Formation. Type section near Gap Creek (NOONKANBAH: 18deg 39' S; 125 deg 55' E). Contains Arenigian brachiopods, trilobites, graptolites & conodonts.||||||23-NOV-17
25894|Emanuel Formation|44236|14|Not recorded|p.173,176|||||||||
25894|Emanuel Formation|44403|2|Defined|opp.p.6, Tb.1|||E/51-12, limestone and shale. U/lain by Precambrian or buried older Palaeozoic rocks. O/lain conformably by Gap Creek Formation.||||||
25894|Emanuel Formation|44404|14|Not recorded|map legend||Ordovician|||||||
25894|Emanuel Formation|44998|2|Defined|18,22,38-9,220-3|||F.4.||||||
25894|Emanuel Formation|45101|6|Mentioned|Fig.28|||||||||
25894|Emanuel Formation|45153|2|Defined|App.1-13|Early Ordovician|Early Ordovician|Formerly Emanuel Limestone. See also App.1-2.||||||
25894|Emanuel Formation|45158|3|Fully described|p28|||||||||
25894|Emanuel Formation|48831|14|Not recorded|p.80|||||||||
25894|Emanuel Formation|50089|5|Briefly described|p427, p428 Fig. 2|Ordovician|Ordovician|Lissoepikodus nudus (conodont) found.  Overlain by Gap Creek Formation. Geological Province: Canning Basin.  See also p430 Fig. 5, p431.||||||
25894|Emanuel Formation|50097|5|Briefly described|p43|Bendigonian|Lancefieldian|Geological Province: Canning Basin. Contains Conodonts. WA.||||||07-FEB-11
25894|Emanuel Formation|62794|5|Briefly described|p298|Early Ordovician|Early Ordovician|Canning Basin. Underlies Gap Creek Formation. Contains trilobites. Cooper (1981) correlated (probably incorrectly) the uppermost Emanuel Formation and the lower half of the Gap Creek Formation with the Horn Valley Siltstone in the Amadeus Basin, NT.||||||05-DEC-12
25894|Emanuel Formation|63121|5|Briefly described|p223|Ordovician|Ordovician|Contains fauna of lingulate brachiopods. Geological Province: Canning Basin.||||||10-NOV-08
25894|Emanuel Formation|63938|5|Briefly described|p48, 51|Ordovician|Ordovician|Of Prices Creek Group. Overlain by Cadjebut Formation in drillholes CD113, CD48.||||||
25894|Emanuel Formation|64334|5|Briefly described|p39-41|Ordovician|Ordovician|Eastern Lennard Shelf, Canning Basin. Arenig.||Prices Creek Group.||Overlies Kudata Dolomite. Is overlain by Gap Creek Formation.|Mudstone.|
25894|Emanuel Formation|64502|6|Mentioned|p769, Fig.6|Ordovician||||||||
25894|Emanuel Formation|64580|6|Mentioned|map legend|||Of Prices Creek Group.||||||15-DEC-08
25894|Emanuel Formation|64643|4|Described|p6, p5 Fig. 4, p21,33, 36 |Ordovician|Ordovician|Of Prices Creek Group. Type section in Emanuel Creek. Poorly exposed siltstone, shale and limestone, lesser sandstone. Abundant macrofossils.||||||
25894|Emanuel Formation|66127|5|Briefly described|p24, Plates 4, 5, 7.|Middle Ordovician|Early Ordovician|||Unit in Prices Creek Group. |||Shallow-marine siltstone, shale and limestone, with lesser sandstone.|
25894|Emanuel Formation|69099|5|Briefly described|500k_geologyp08_lut.csv|Middle Ordovician|Early Ordovician|||Prices Creek Group||||
25894|Emanuel Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Ordovician|Ordovician|||Prices Creek Group||||
25894|Emanuel Formation|69883|5|Briefly described|p4-p5|Arenig|Arenig|Canning Basin. Conodont zones and supersequences provided.||Prices Creek Group||Overlies the Kudata Dolomite. Overlain by the Gap Creek Formation.|Carbonate and mudstone.|
25894|Emanuel Formation|71171|5|Briefly described|p2, p5|||Canning Basin. The lower part of this unit has been renamed the Kunian Sandstone.||||||
25894|Emanuel Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Prices Creek Group.|||Fossiliferous shallow marine limestone and interbedded shale|
25894|Emanuel Formation|72497|5|Briefly described|p3 Fig.2.|Early Ordovician|Early Ordovician|Shown as occuring as part of the Lennard Shelf and Margaret Terrace.||||Conformably underlies Gap Creek Formation.||
25894|Emanuel Formation|73344|5|Briefly described|p3-4, p6, p41, p51, p56, p63-64|Floian|Tremadocian|Canning Basin, Lennard Shelf. Defined by Guppy and Opik (1950); amended by Guppy et al. (1958). Type section from 594 m of outcrop near Emanuel Creek. Part of supersequence A0. The Prioniodus adami - S. bilobatus biozone is identified in the middle and upper portion.||Prices Creek Group||Underlain by Kudata Dolomite. Overlain by Gap Creek Formation. Equivalent to Samphire Marsh Member and Fly Flat Member[?] (Nambeet Formation), and Wilson Cliffs Sandstone.||
25894|Emanuel Formation|73567|6|Mentioned|p62, p68-69|Ordovician|Ordovician|Canning Basin, Lennard Shelf.||Prices Creek Group||Equivalent to the Nambeet Formation.||
40510|Emerald Mine Greenstone Complex|24531|5|Briefly described|p7, p9|Archean|Archean|Overlies the Warrawoona and Gorge Creek Groups.||||||07-NOV-08
28532|Emeriau Sandstone|7433|5|Briefly described|p25 Fig.2,  p42, pp45-46.|Cretaceous|Cretaceous|Canning Basin. Fluvial clastics. 30 m or more thick. Possibly equivalent to Frezier Sandstone.||||Disconformably overlies Broome and Melligo Sandstones in far north of the basin.|Sandstone; ferruginised by weathering.|
28532|Emeriau Sandstone|22718|5|Briefly described|P8, Table1 P6||Early Cretaceous|Equivalent to Frezier Sandstone.||||||01-OCT-08
28532|Emeriau Sandstone|22776|6|Mentioned|p11, Table.3|||||||||
28532|Emeriau Sandstone|32648|6|Mentioned|p32|||Tertiary||||||
28532|Emeriau Sandstone|36890|4|Described|p355|||||||||
28532|Emeriau Sandstone|38878|6|Mentioned|Map legend|Aptian|Neocomian|Neocomian - Aptian||||||
28532|Emeriau Sandstone|38886|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
28532|Emeriau Sandstone|40045|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
28532|Emeriau Sandstone|42571|5|Briefly described|Table1 P8|||||||||
28532|Emeriau Sandstone|42930|5|Briefly described|Fig.1 P473|Tertiary|Tertiary|Geological Province: Canning Basin.||||||13-NOV-07
28532|Emeriau Sandstone|44143|4|Described|p.431 Table 4-19|Cretaceous|Cretaceous|Up to 30m thick; fine to coarse sandstone, minor conglomerate; fluvial. Disconformably overlies Melligo and Broome Sandstones. Type section at Emeriau Point  (PENDER: 16deg 46' S, 122deg 34' E).||||||23-NOV-17
28532|Emeriau Sandstone|44998|2|Defined|p196,199||Tertiary|Overlies Broome Sandstone and Jowlaenga Formation.||||||13-NOV-07
28532|Emeriau Sandstone|45153|2|Defined|App.10-154|early Tertiary|Late Cretaceous|Late Cretaceous to Early Tertiary.||||||13-NOV-07
28532|Emeriau Sandstone|45158|3|Fully described|p12|||||||||
28532|Emeriau Sandstone|64449|5|Briefly described|p62 Tb. 2|Mesozoic|Mesozoic|Consists of cross-bedded, poorly sorted sandstone, and minor conglomerate.||||||07-FEB-11
28532|Emeriau Sandstone|64580|4|Described|map legend||Early Cretaceous|Fine- to coarse-grained sandstone; minor conglomerate.||||||15-DEC-08
28532|Emeriau Sandstone|69182|6|Mentioned|Ch4 p3|||Canning Basin. ||||||
28532|Emeriau Sandstone|69590|4|Described|500k_geologyp08_lut.csv||Early Cretaceous||||||Fine- to coarse-grained sandstone; minor conglomerate|
28532|Emeriau Sandstone|70154|5|Briefly described|500k_interpgeop14_lut.csv|Neogene|Lower Cretaceous||2.6-145 Ma||||Fine- to coarse-grained sandstone; minor conglomerate|
28532|Emeriau Sandstone|71267|4|Described|GEOL_LUT_CSV files|Neogene|Early Cretaceous|Of Canning Basin. See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|145-2.58 Ma (inferred)||||Fine- to coarse-grained poorly sorted sandstone; conglomerate|
28532|Emeriau Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Neogene|Early Cretaceous|Canning Basin.|||||Fine- to coarse-grained sandstone; minor conglomerate.|
23579|Emma Member|42615|4|Described|p32|||of Calypso Formation. Reserved.||||||
23579|Emma Member|68135|5|Briefly described|p51 fig 2a|Callovian|Callovian|Northern Carnarvon Basin.||Calypso Formation.||||14-SEP-17
76051|Emu Point Member|64748|4|Described|p268 Fig1, p269 Fig 2,3,Tb.1, p270, 277|||Of King Leopold Sandstone, Kimberley Group. Glaciofluvial; pebble conglomerate and coarse-grained sst; unconformably/disconformably overlies Bedford Sandstone; 1-15m thick; poorly-sorted quartz-pebble and sst-boulder conglomerate||||||
76051|Emu Point Member|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||King Leopold Sandstone.|||Pebble and cobble conglomerate, boulder conglomerate; clasts of quartz and siliciclastic sedimentary rock; coarse-grained sandstone interbeds.|
68766|Emu Pool Supersuite|63417|5|Briefly described|Map legend|Archean|Archean|Includes 15 named granites. Ages ranges from 3324-3310Ma to 3299-3290Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
68766|Emu Pool Supersuite|63420|5|Briefly described|Map legend|Archean|Archean|Includes Coppin Gap Granodiorite and Munganbrina Monzogranite and four unnamed monzogranites. Ages of two of units: c.3314Ma and3303Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
68766|Emu Pool Supersuite|63441|5|Briefly described|p35, p8 Tb. 2|Archean|Archean|Includes some 19 granites. Age: 3325-3290Ma. Geological province: East Pilbara Terrane/Pilbara Craton. Dominantly monzogranitic rocks - from trondhjemite to syenogranite. See also p31 Fig. 10.||||||07-FEB-11
68766|Emu Pool Supersuite|63538|6|Mentioned|p6 Fig. 3|Archean|Archean|Geological Province: Pilbara Craton.||||||19-APR-13
68766|Emu Pool Supersuite|64405|5|Briefly described|p15|Archean|Archean|Intrusive. Age: c.3310Ma.||||||07-FEB-11
68766|Emu Pool Supersuite|64580|6|Mentioned|map legend|||||||||
68766|Emu Pool Supersuite|64621|5|Briefly described|Map legend|Archean|Archean|Contains 9 named granites with ages ranging from 3321ma to 3300Ma. Unnamed granites also included.||||||07-NOV-08
68766|Emu Pool Supersuite|65724|5|Briefly described|map legend|Paleoarchaean|Paleoarchaean|Includes Elsie Creek Tonalite. Geol. Prov: East Pilbara Granite-Greenstone Terrane.||||||
68766|Emu Pool Supersuite|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. This name has replaced the Mount Edgar and Corunna Downs Granitoid Complexes which were used on Version 1 of this map (see Refid 65726), although some units have been re-assigned elsewhere.|c.3324 - 3294 Ma.||Includes Wilina, Joorina, Chessman, Kennell, Coppin Gap, Gobbos, Mullugunya and Zulu Granodiorites; Davitt Syenogranite; Carbana and Munganbrina Monzogranites; Walgunya and Chimingadgi Trondhjemites.|||
68766|Emu Pool Supersuite|65825|6|Mentioned|p32.|||Appendix 2 indicates that this unit includes rocks, now called the Elsie Creek Tonalite, which used to be un-named within the Yilgalong Granitic Complex, according to the GSWA databases.|||Includes Elsie Creek Tonalite.|||
68766|Emu Pool Supersuite|65827|4|Described|p6 Tb.2, p9 Fig.3, p15-16, p22-26,p57-58|Paleoarchean|Paleoarchean|3325-3290 Ma. Of Mount Edgar Granitic Complex, Corunna Downs Granitic Complex. Includes Zulu, Mullugunya, Coppin Gap, Kennell, Gobbos, Chessman, Joorina and Wilina Granodiorites; Chimingadgi and Walgunya Trondhjemites; Munganbrina and Carbana Monzogranites; and Davitt Syenogranite. Intrudes Callina and Tambina Supersuites; intruded by Cleland Supersuite.||||||
68766|Emu Pool Supersuite|65829|5|Briefly described|p1, p7 Fig.3, pp11-12. |Paleoarchean|Paleoarchean|Granitic intrusives.|3325 - 3290 Ma (Van Kranendonk et al. 2006).||Includes Elsie Creek Tonalite.|||
68766|Emu Pool Supersuite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Includes Triberton, Nandingarra, Kennell, Joorina, Jenkin, Cotton Well and Campbell Well Granodiorites; Munganbrina, Johansen and Carbana Monzogranites; Boobina Porphyry; unnamed meta monzogranite-granodiorite unit.||||||
68766|Emu Pool Supersuite|66217|4|Described|p1, p5, p6 Table 1, p10-11, p14, pp32-34|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Predominantly potassic. Derived from partial melting of older granitic supersuites, and emplaced during episodes of partial convective overturn of the upper and middle crust, during eruption of the Wyman Formation.|3325-3290 Ma.|Unit in Mount Edgar and Corunna Downs Granitic Complexes.|Includes Munganbrina Monzogranite and Coppin Gap Granodiorite.|Intrudes Pilbara Supersuite.|Strongly foliated and folded granitic rocks (tonalite through monzogranite).|
68766|Emu Pool Supersuite|67201|6|Mentioned|p7 Fig.5, p11|||Thermal event resposible for Kelly Group and Emu Pool Supersuite ceased at c. 3290 Ma.||||||
68766|Emu Pool Supersuite|68035|5|Briefly described|p286 Fig 3|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. |3.32 - 3.29 Ga|||||
68766|Emu Pool Supersuite|68280|6|Mentioned|p3|Paleoarchean|Paleoarchean||3320-3290 Ma|||||
68766|Emu Pool Supersuite|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c.3314 - c.3303 Ma||Includes Coppin Gap Granodiorite, Munganbrina Monzogranite, Gap Intrusion, Strutton Intrusion.||Monzogranites, granodiorite; serpentinized dunite and serpentine schist, metagabbro and metapyroxenite.|06-JAN-15
68766|Emu Pool Supersuite|69012|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane. Nine unnamed sub-units are mapped separately.|||Includes Nandingarra Granodiorite, Boobina Porphyry, Carbana Monzogranite, and Triberton Granodiorite.|||28-APR-14
68766|Emu Pool Supersuite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Also includes Campbell Well Granodiorite, Jenkin Granodiorite, Munganbrina Monzogranite, Nandingarra Granodiorite, Gobbos Granodiorite, Carbana Monzogranite, Kennell Granodiorite, Coppin Gap Granodiorite, Joorina Granodiorite, Wilina Granodiorite, Chimingadgi Trondhjemite, Davitt Syenogranite, Triberton Granodiorite, Walgunya Trondhjemite. |||Includes Elsie Creek Tonalite, Zulu Granodiorite, Johansen Monzogranite, Mullugunya Granodiorite||Hornblende--biotite monzogranite; fine- to coarse-grained, seriate to plagioclase-porphyritic. Strongly foliated to schistose metamonzogranite; fine to medium grained. Granodiorite, leucocratic monzogranite and syenogranite.|
68766|Emu Pool Supersuite|69185|5|Briefly described|500k_geologyp08_lut.csv|||Geological Province: Pilbara Craton.|||Includes Coppin Gap Granodiorite, Gobbos Granodiorite.|||
68766|Emu Pool Supersuite|69301|6|Mentioned|p5 Fig.3|||Pilbara Craton. East Pilbara Terrane. Pilbara Supergroup successions include thick felsic volcanic formations, each contemporaneous with the four granitic supersuites. i.e. Wyman Formation and Emu Pool Supersuite.||||||
68766|Emu Pool Supersuite|69566|5|Briefly described|p236-237, 248|||Mount Edgar Granitoid Complex, East Pilbara Granite-Greenstone Terrane. Sagduction involves a burst of magmatic activity coeval with fast burial and exhumation of crustal rocks, followed by a long period of tectonic quiescence.|3324-3290 Ma.||Wilina, Joorina, Chessman, Kennell, Jenkin Granodiorites.||Voluminous granodioritic plutons.|
68766|Emu Pool Supersuite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Also includes MONZOGRANITES: Carbana, Johansen, Munganbrina; TRONDHJEMITES: Chimingadgi, Walgunya; Davitt Syenogranite, Elsie Creek Tonalite..See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|3324-3277 Ma (inferred)||Includes Boonina Porphyry; GRANODIORITES: Campbell Well, Chessman, Coppin Gap, Cotton Well, Gobbos, Jenkin, Joorina, Kennell, Mullugunya, Nandingarra, Triberton, Wilina, Zulu.||Monzogranite; granophyric, leucocratic, porphyritic and seriate, metamorphosed; granodiorite, syenogranite, tonalite to quartz diorite.|
68766|Emu Pool Supersuite|70022|6|Mentioned|p115|||East Pilbara Terrane.||||||
68766|Emu Pool Supersuite|70775|5|Briefly described|p23|||Similar in age to six xenocrystic zircons from the Karratha Granodiorite which were dated between 3332 and 3287 Ma.||||||
68766|Emu Pool Supersuite|70884|5|Briefly described|p122-123,135|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Associated with post-Strelley Pool Formation D3 deformation.|3.33-3.29 Ga|||||
68766|Emu Pool Supersuite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, tonalite, quartz diorite, syenogranite|
68766|Emu Pool Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Includes Elsie Creek Tonalite, Zulu, Mullugunya, Nandingarra, Joorina, Jenkin, Cotton Well, Campbell Well, Wilina, Kennell, Gobbos, Coppin Gap, Chessman, Triberton Granodiorites, Boobina Porphyry,  Johansen, Munganbrina, Carbana Monzogranites, Chimingadgi, Walgunya Trondhjemites, Davitt Syenogranite.|Max age 3324+/-6 Ma, Min 3277+/-4 Ma.||Includes 21 tonalites, granodiorites, monzogranites, trondhjemites and syenogranites.||Monzogranite and granodiorite; minor trondhjemite; metamorphosed.|
68766|Emu Pool Supersuite|72251|5|Briefly described|p52-54,65|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Granitic supersuite with Nd model age of ~4.1-3.4 Ga (Smithies et al., 2003, 2007; Champion, 2013).|3.32-3.29 Ga||||Granodiorite and monzogranite.|
68766|Emu Pool Supersuite|72668|6|Mentioned|p5, p9-11, p18-19, p26|||East Pilbara Terrane. Genetically related to the Wyman Formation. Appears as the Emu Supersuite on p19.|c. 3325-3290 Ma||||Dominantly monzogranitic. Compositions range from trondhjemite to diorite to syenite.|13-JAN-22
68766|Emu Pool Supersuite|73598|6|Mentioned|p1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.||||||
34449|Emull Gabbro|22754|6|Mentioned|p23|||||||||
34449|Emull Gabbro|23383|4|Described|p13, p5 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Sally Downs supersuite (Lamboo Complex).  Comprises medium- to fine-grained, subophitic and subhedral granular gabbro, xenocrystic quartz gabbro and tonalite.Geological Province: Halls Creek Orogen.||||||07-NOV-08
34449|Emull Gabbro|23599|5|Briefly described|p12|Paleoproterozoic|Paleoproterozoic|Age: 1820-1805 Ma. See also page 5 Table 1.||||||07-NOV-08
34449|Emull Gabbro|23601|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Medium- to fine-grained gabbro, quartz gabbro, and tonalite; extensively veined by the Dillinger Monzogranite, aplite, quartz-feldspar porphyry, and pegmatite.||||||07-NOV-08
34449|Emull Gabbro|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  Medium- to fine-grained gabbro, quartz gabbro, and tonalite; extensively veined by Dillinger Monzogranite, aplite, quartz-feldspar porphyry, and pegmatite. Age: c.1835-1805Ma. Part of the Bow River batholith.||||||07-NOV-08
34449|Emull Gabbro|44694|5|Briefly described|Map Legend||Proterozoic|||||||
34449|Emull Gabbro|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Sally Downs Supersuite|||Microgabbro, quartz microgabbro, and microtonalite; extensively veined by the Dillinger Monzogranite and leucocratic granite|31-JUL-15
34449|Emull Gabbro|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Sally Downs Supersuite||Intruded by Dillinger Monzogranite|Microgabbro, quartz microgabbro and microtonalite.|
34449|Emull Gabbro|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2.|1832-1808 Ma (Inferred)|Unit of Sally Downs Supersuite.|||Microgabbro, quartz microgabbro, and microtonalite; extensively veined by the Dillinger Monzogranite and leucocratic granite|
34449|Emull Gabbro|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1808-1832 Ma|Sally Downs Supersuite|||Microgabbro, quartz microgabbro, microtonalite, extensively veined leucocratic granite and monzogranite.|
34449|Emull Gabbro|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1832+\3 to 1808+\-3 Ma (inferred)|Unit of Sally Downs Supersuite.|||Microgabbro, quartz microgabbro, and microtonalite; extensively veined by the Dillinger Monzogranite and leucocratic granite|
34449|Emull Gabbro|72437|5|Briefly described|p93|||Whole rock analyses are provided.||Sally Downs Supersuite|||Biotite amphibolite and biotite gabbronorite.|
25897|Enacheddong Dolomite|41669|2|Defined|Table 5|Precambrian?||Fully described p39||||||24-MAY-19
25897|Enacheddong Dolomite|41768|4|Described|p40|||||||||
25897|Enacheddong Dolomite|43055|3|Fully described|Table 4, Table 5|||of Manganese Group||||||
25897|Enacheddong Dolomite|43056|5|Briefly described|Map Legend|||of Manganese Group||||||
25897|Enacheddong Dolomite|44142|5|Briefly described|p315-316 Tb.4-4, p323|||Up to 350m thick lenticular unit; dominantly marine slope deposits. Distinctive banded photo pattern. Stromatolites not found.||Manganese Subgroup||Overlies Stag Arrow Formation conformably. Overlain conformably by Jigalong and Balfour Formations.|Multi-coloured, thin-bedded to laminated dolomite, ferruginous shale, banded chert.|13-MAR-18
25897|Enacheddong Dolomite|67183|5|Briefly described|p645|Mesoproterozoic|Mesoproterozoic|Present in the Oakover Basin. Creatively mis-spelt as Enachedong (p645 Tb.1, p649 Fig.8, p671), Enechadong (p643 Fig.3) and Ennechadong (p649 Fig.8), Dolomite.||Manganese Subgroup|||Silty dolomite, <300 m thick laminated dolomite and siltstone sequence.|
25897|Enacheddong Dolomite|71042|4|Described|p66 fig 2, p67|Mesoproterozoic|Mesoproterozoic|Oakover Basin. <300m thick. Misspelt as Enachedong Dolomite in Fig 2||Manganese Group||Overlies the Stag Arrow Formation. Overlain by the Balfour Formation.|Laminated dolomite and siltstone.|28-MAY-19
25897|Enacheddong Dolomite|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||shale, dolarenite, cherts, crystalline dolostone/dolomite|
29284|Eneabba Formation|12758|4|Described|p16, p3 Fig. 3|Early Jurassic|Early Jurassic|Formerly the "Multicoloured Member" of the Cockleshell Gully Fm.  Feldspathic sandstone interbedded with local minor conglomerate and multicoloured claystone and siltstone. Conformably overlies Cattamarra Coal Measures. Geol. Province:  Perth Basin.||||||11-APR-08
29284|Eneabba Formation|14227|5|Briefly described|p8, p10|Jurassic|Early Jurassic|Overlain by Cattamarra Coal Measures; overlies, transitionally, the Lesueur Sandstone. Non-marine red bed sedimentation, including multi-coloured silts and clays, with some channel sands. See also Enclosure 2.||||||07-FEB-11
29284|Eneabba Formation|14228|6|Mentioned|p5 fig 2|Early Jurassic|Early Jurassic|||||Overlies Lesueur Sandstone.||
29284|Eneabba Formation|22814|5|Briefly described|fig2|Jurassic|Jurassic|||||||
29284|Eneabba Formation|23172|4|Described|Map Legend|Jurassic|Jurassic|||||||
29284|Eneabba Formation|23279|4|Described|p24-7||Early Jurassic|||||||
29284|Eneabba Formation|23520|5|Briefly described|p6 Fig. 4|Early Jurassic|Late Triassic|Geological Province: Abrolhos Sub-basin.  See also p9 and p21.||||||
29284|Eneabba Formation|24390|5|Briefly described|p15 Fig. 8|Jurassic|Triassic|Geological Province: Perth Basin.||||||
29284|Eneabba Formation|24443|5|Briefly described|Fig.30, 31|Early Jurassic|Late Triassic|Overlies Lesueur Sandstone. Overlain by Cattamarra Coal Measures. Geological Province: Bight Basin.||||||
29284|Eneabba Formation|42687|6|Mentioned|map legend|Jurassic||Variation on Eneabba Member.||||||
29284|Eneabba Formation|42688|6|Mentioned|map legend|Jurassic||||||||
29284|Eneabba Formation|43197|5|Briefly described|Map Legend||Jurassic|||||||
29284|Eneabba Formation|43216|5|Briefly described|Map Legend||Jurassic|Perth Basin.||||||11-APR-08
29284|Eneabba Formation|43217|5|Briefly described|Map Legend||Jurassic|Perth Basin||||||
29284|Eneabba Formation|43296|5|Briefly described|Map Legend||Jurassic|||||||
29284|Eneabba Formation|43297|4|Described|p10,Fig.3 p5.||Early Jurassic|See also Table 1 p6,p10.Type section location given.||||||11-APR-08
29284|Eneabba Formation|43347|1|Redefined|5||Early Jurassic|Previously Member of Cockleshell Gully Formation (abandoned).||||||13-DEC-22
29284|Eneabba Formation|43495|4|Described|6-36|Sinemurian|Norian|||||||
29284|Eneabba Formation|43504|4|Described|4-10|Sinemurian|Hettangian|||||||
29284|Eneabba Formation|49942|5|Briefly described|p4 Fig.3|Early Jurassic|Early Jurassic|Conformably overlies Lesueur Sandstone. Geological Province: Gascoyne Platform.||||||
29284|Eneabba Formation|50085|5|Briefly described|p15 Fig. 8|Jurassic|Triassic|Geological Province: Northern Perth Basin.||||||11-MAY-04
29284|Eneabba Formation|50107|5|Briefly described|Map legend|Jurassic|Jurassic|Geological Province: Perth Basin.||||||
29284|Eneabba Formation|60118|6|Mentioned|p29|||Geological Province: Perth Basin.||||||
29284|Eneabba Formation|60376|4|Described|p16, p17 Fig. 4. |Early Jurassic|Early Jurassic|Geological Province: Perth Basin. Overlain by Cattamarra Coal Measures. Underlain unconformably by Lesueur Sandstone. Fine to coarse-grained sandstone, shales and some thin coals and calcareous siltstones.||||||07-FEB-11
29284|Eneabba Formation|60384|6|Mentioned|p243 Fig 2a, p261|Early Jurassic|Late Triassic|Perth Basin. Potential reservoir.||||||
29284|Eneabba Formation|60386|6|Mentioned|p299|Early Jurassic|Early Jurassic|Perth Basin. Non-marine.||||||
29284|Eneabba Formation|61023|5|Briefly described|p20 Fig 10|Jurassic|Triassic|Geological Province: Perth Basin.||||||11-APR-08
29284|Eneabba Formation|61811|5|Briefly described|p3 Fig.2, p63.|Early Jurassic|Late Triassic|Northern Perth Basin. Type section details in Appendix 1.||||Overlies Lesueur Sandstone. Is overlain by Cattamarra Coal Measures.||
29284|Eneabba Formation|64580|4|Described|map legend||Middle Jurassic|Interbedded red-bed sandstone and siltstone.||||||15-DEC-08
29284|Eneabba Formation|64635|5|Briefly described|p4 Fig.3 |Sinemurian|Norian|||||Overlies Lesueur Sandstone. Is overlain by Cattamarra Coal Measures.||
29284|Eneabba Formation|67135|5|Briefly described|p5 Fig.7, p33 Fig.42.|Jurassic|Triassic|Perth Basin. Mis-spelled as Enebba Formation in Fig.42.||||Overlies Lesueur Sandstone. Is overlain by Cattamarra Coal Measures.||
29284|Eneabba Formation|67340|6|Mentioned|p6-8|Jurassic|Triassic|Northern Perth Basin. See also references to Eneabba Member (p8, 25, 50-63).||||||
29284|Eneabba Formation|67370|6|Mentioned|p323 Fig.14.|Jurassic|Jurassic|||||||
29284|Eneabba Formation|67888|6|Mentioned|p82|||||||||
29284|Eneabba Formation|67925|5|Briefly described|Ch2 p10 fig 4, Ch3 p8, Ch4 p8 fig 2|Sinemurian|Hettangian|Referred to as the obsolete Eneabba Member on Ch4 p8 fig 2.  ||||Overlies the Lesueur Sandstone, Myalup Member. Overlain by the Cattamarra Coal Measures.||
29284|Eneabba Formation|69029|6|Mentioned|p332|Sinemurian|Hettangian|Of Perth Basin.||||Overlain by Cattamarra Coal Measures. Underlain by Lesueur Sandstone.||
29284|Eneabba Formation|69081|5|Briefly described|p736,p740,p741, Figs.3 and 4, Tbs.1-3|Early Jurassic|Early Jurassic|Presented as Eneabba Fm in figure. Geol. Prov: Perth Basin||||is overlain by Cattamarra Coal Measures; overlies Yalgorup Member (Lesueur Sandstone)||
29284|Eneabba Formation|69182|5|Briefly described|p7, Ch2 p3, Ch2 p9, Ch2 p14|Early Jurassic|Early Jurassic|Perth Basin. Forms a regional seal along with the Cadda Formation. See also  Ch2 p20-p29, Ch2 p34-p42, Ch2 p44-p46, Ch2 p52-53, Ch2 p55, Ch2 p57, Ch2 p60-p63, Ch2 p70-p74, Ch2 p76, Ch2 p84-p86, Ch2 p93, Ch2 p101, Ch2 p105, Ch2 p109, Ch3 p12.||||Overlies the Lesueur Sandstone, Upper. Overlain by the Cattamarra Coal Measures.|Fluvial sediments and red beds.|
29284|Eneabba Formation|70097|5|Briefly described|p2, p4, p7, p19-21 Figs.3-5|Toarcian|Rhaetian|Minor phase of west-northwest to east-southeast extension in Perth Basin, reactivated a number of faults in the basin, with syn-tectonic deposition of non-marine red beds, during latest Triassic to Early Jurassic. Rifting appears to occur in onshore part of basin. Greenough/Bookara Shelf, Dongara Saddle, Dandaragan Trough, Beermullah Trough and Mandurah Terrace.||||Overlies Lesueur Sandstone. Is overlain by Cattamarra Coal Measures.|Non-marine red beds. Includes siltstone.|12-SEP-17
29284|Eneabba Formation|70128|5|Briefly described|p449, p454, p457, p459-464|Early Jurassic|Early Jurassic|Perth Basin. Modelled thickness distribution histogram. Has minimal unconformities: has undergone no significant erosion. Thickness differences indicate locally heterogeneous subsidence.||||Unconformably overlies Lesueur Sandstone. Is overlain conformably by Cattamarra Coal Measures.||
29284|Eneabba Formation|70796|5|Briefly described|500k_interpgeop14_lut.csv|Lower Jurassic|Lower Jurassic|Perth Basin. Formed during Gondwana breakup along the western margin.|201.3  174.1 Ma (biostrat)||||Interbedded redbed sandstone and siltstone.|
29284|Eneabba Formation|70826|6|Mentioned|p7 tbl 4|Jurassic|Jurassic|Perth Basin.||||||
29284|Eneabba Formation|71146|6|Mentioned|p16 fig 10|Jurassic|Jurassic|Northern Perth Basin. ||||||
29284|Eneabba Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone, coal|
29284|Eneabba Formation|71269|4|Described|500k_interpgeop16_lut.csv|Early Jurassic|Early Jurassic|Of Perth Basin. Events: Mid-Miocene transgression, 15 Ma (15-15 Ma); Wilson Bluff transgression, 42 Ma (42-42 Ma); Kings Park transgression, 56 Ma (56-56 Ma); Gondwana breakup-western margin (210-125 Ma); Jurassic-Early Cretaceous rifting, Perth Basin (168-133 Ma);??|201.4-174.1 Ma (biostrat)||||Interbedded red-bed sandstone and siltstone|
29284|Eneabba Formation|71377|4|Described|p1-p3, p7, p9, p17-p22|Early Jurassic|Early Jurassic|Perth Basin. SHRIMP ages are interpreted as the maximum depositional ages derived from detrital zircons in this study. Two additional ages are provided at 514 +/- 15 Ma and 505 +/- 23 Ma. These dates are considerably older than the biostratigraphic Early Jurassic age. Intersected in GSWA Harvey 1 (249-700m) where it is described. Interpreted to have been deposited in a fluvial environment. Zircon morphology and sample descriptions are provided. See also p25-p30, p33-p38, p85, p87-p88, p90, p103-p104.|515 +/- 11 Ma (SHRIMP U-Pb)|||Conformably overlies the Yalgorup Member of the Lesueur Sandstone. Conformably overlain by the Cattamarra Coal Measures. Unconformably overlain by the Leederville Formation.|Coarse to very coarse-grained sandstone interbedded with multi-coloured claystone and siltstone, local conglomerate.|06-OCT-20
29284|Eneabba Formation|71958|5|Briefly described|p34|Sinemurian|Hettangian|Vlaming Sub-basin.||||Overlies the Myalup Member (Lesueur Sandstone). Overlain by the Cattamarra Coal Measures.||
29284|Eneabba Formation|72034|5|Briefly described|500k_interpgeop16_lut|Early Jurassic|Early Jurassic|Perth Basin.  Age from biostratigraphy.|||||Interbedded red-bed sandstone and siltstone.|
29284|Eneabba Formation|72258|5|Briefly described|p129,133,138|Early Jurassic|Early Jurassic|Of Perth Basin. Major peak in Mesoproterozoic (1300-1100 Ma) and subordinate Late Paleoproterozoic (1800-1600 Ma) detrital zircons correlate with characteristic ages and Hf isotopic signatures of magmatism in the Albany-Fraser-Wilkes Orogen (Clark et al., 2000; Fitzsimons, 2000, 2003; Kirkland et al., 2011; Spaggiari et al., 2015). Late Meso- to Early Neoproterozoic (1100-900 Ma) detrital zircons atributed to Pinjarra Orogen. Neoproterozoic 600-500 Ma peak in detrital zircon ages also likely to be derived locally from Pinjarra Orogen (p134-135 describes potential, but unlikely Gondwanan sources). Demonstrates up-sequence increase in Archean and Ediacaran-Cambrian detritus from the Lower Triassic Sabina Sandstone to Lower Jurassic Eneabba Formation. ||||Overlain by, and laterally grades southward into Cattamarra Coal Measures. Underlain by Lesueur Sandstone.||
29284|Eneabba Formation|73424|6|Mentioned|p5|Early Jurassic|Early Jurassic|Perth Basin.||||||
29284|Eneabba Formation|73513|5|Briefly described|p30 Fig.2|Pliensbachian|Norian|Perth Basin.||||Overlies Lesueur Formation, underlies Cattamarra Coal Measures|Fluvial unit.|
79245|Eneabba Sequence|69297|5|Briefly described|p175, p189, p202, p204|Pleinsbachian|Rhaetian|Vlaming Sub-basin, South Perth Basin. See also p206, p207, p209, p223, p225, p236, p238. ||||Overlies the Lesueur Sequence. Overlain by the Cattamarra Sequence.|Fluvial sandstone interbedded with varicoloured siltstone and claystone.|
79245|Eneabba Sequence|70097|6|Mentioned|p4|Early Jurassic|Early Jurassic|Offshore Perth Basin.||||||20-OCT-15
69188|Enterprise Dolerite|60514|5|Briefly described|p65 Table 1.|Archean|Archean|Of the Grants Patch Group. Overlain by Mt Pleasant Sill and Bent Tree Basalt, underlain by Linger and Die Group. Geological Province: Ora Band Domain.||||||07-FEB-11
69188|Enterprise Dolerite|60627|5|Briefly described|p65 Tb.1|||Intrudes Grants Patch Group. See also Mount Ellis Sill.||||||
69188|Enterprise Dolerite|70326|6|Mentioned|p362|Neoarchean|Neoarchean|Geological province: Ora Banda region, Ora Banda Domain, Kalgoorlie Terrane, Yilgarn Craton.||||||
69188|Enterprise Dolerite|72049|5|Briefly described|p258|||St Ives area, occurs in the upper parts of the Kambalda Sequence.||||Intrudes the Kambalda Sequence.|Doleritic rocks.|
69188|Enterprise Dolerite|73391|6|Mentioned|p53, Appendices.|||Ora Banda Domain, Kalgoorlie Terrane.||||||
68508|Eramurra Monzogranite|63441|2|Defined|p10 Tb. 2, p37|Archean|Archean|Of the Maitland River Supersuite. Age: 2982+/-5Ma. Geological province: Pilbara Craton. Composite, including pegmatite veins of Sisters Supersuite rock.||||||07-FEB-11
68508|Eramurra Monzogranite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Maitland River Supersuite. Geological province: Pilbara Craton.  Seriate biotite monzogranite containing mafic schlieren and veins of pegmatite; metamorphosed.||||||07-NOV-08
68508|Eramurra Monzogranite|64580|4|Described|map legend||Mesoarchean|Of Maitland River Supersuite. Seriate biotite monzogranite containing mafic schlieren and veins of pegmatite; metamorphosed.||||||15-DEC-08
68508|Eramurra Monzogranite|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Maitland River Supersuite.|||Seriate biotite monzogranite containing mafic schlieren and veins of pegmatite; metamorphosed|
68508|Eramurra Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
68508|Eramurra Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|De Grey Superbasin.|2982+/-5 Ma|Maitland River Supersuite|||Seriate biotite monzogranite containing mafic schlieren and veins of pegmatite; metamorphosed.|
33441|Erong Granite|23781|5|Briefly described|p40|Paleoproterozoic|Paleoproterozoic|Age: c.1800Ma.||||||07-NOV-08
33441|Erong Granite|24544|4|Described|p16|Paleoproterozoic|Paleoproterozoic|Age: c. 1800 Ma. Medium- to coarse-grained muscovite-biotite-garnet monzogranite, granite and pegmatite. Intrudes Petter Calc-silicate.||||||07-NOV-08
33441|Erong Granite|63246|6|Mentioned|p490|||Cuts through Palaeoproterozoic structures in the Earabiddy Shear Zone.||||||
33441|Erong Granite|63866|5|Briefly described|p159, p177|||Age interpreted from correlations with similar granites in the region.|c. 1800 Ma (Nelson, 2000)|||Intrudes the Camel Hills Metamorphics.|Muscovite-biotite-garnet monzogranite to pegmatite.|
33441|Erong Granite|66299|6|Mentioned|p99.|||Contains a raft of Petter Calc-silicate rock, about 2.5 km north-northwest of Erong Homestead.||||||
33441|Erong Granite|67843|6|Mentioned|p10.|||Includes a raft of Petter Calc-silicate, 2.5 km NNW of Erong homestead.||||||
33441|Erong Granite|69387|6|Mentioned|p12|||Errabiddy Shear Zone.||Moorarie Supersuite.||||
33441|Erong Granite|72259|6|Mentioned|App. Tb.B||||||||Includes biotite-muscovite-garnet granodiorite.|
77579|Esko Bed|66127|5|Briefly described|p422.|Frasnian|Frasnian|A white to yellowish-grey scutelluid marker bed on McWhae Ridge, just above the cliff of the Lower Beloceras Bed, Canning Basin. Contains a new involute species of Clauseniceras. See also Fig 2.1 p432 and location description p417.||Virgin Hills Formation||||31-JAN-14
78596|Esperance Supersuite|65487|4|Described|p 52-55, 1, p9, 24, 56 Fig. 27|Mesoproterozoic|Mesoproterozoic|Formerly the Esperance Granite. Included as part of the Kepa Kurl Booya Province; c.1140 Ma intrusion, coincides with Stage II of the Albany-Fraser Orogeny. SHRIMP U-Pb zircon ages of 1135 +/- 56 Ma and 1138 +/- 38 Ma (Nelson, 1995). Relatively undeformed, low metamorphic grade, granitic rocks that intrude the Recherche Supersuite.||||Intrudes Recherche Supersuite rocks.||16-JAN-14
78596|Esperance Supersuite|67268|5|Briefly described|p3, p8, p9, p10, p17|Mesoproterozoic|Mesoproterozoic|Biranup Zone. Relatively undeformed and intruded during later stages of the Albany-Fraser Orogeny.|1299 +/-18 Ma (SHRIMP U/Pb), 1283 +/- 13 Ma|||Intrudes Coramup Gneiss, Salisbury Gneiss, Mount Ragged Formation||15-JUN-22
78596|Esperance Supersuite|67380|6|Mentioned|p5-6|Stenian|Stenian|Albany-Fraser Orogen.|c.1140 Ma.|||||
78596|Esperance Supersuite|67581|6|Mentioned|p47||||c.1140 Ma; Kirkland et al. (2011).|||||
78596|Esperance Supersuite|67722|5|Briefly described|p1, p12, 15, 17|Mesoproterozoic|Mesoproterozoic|Nornalup Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen. |c. 1140 Ma||||Igneous rocks metamorphosed through greenschist-amphibolite facies.|
78596|Esperance Supersuite|67888|6|Mentioned|p61|Mesoproterozoic|Mesoproterozoic||c. 1140 Ma|||||
78596|Esperance Supersuite|68186|4|Described|p3 Fig.2, p4, p7-9, p11, p17, p19,p26-29|Mesoproterozoic|Mesoproterozoic|See also p33, p40-41, Plates 1A, 2. Nornalup Zone and SE Biranup Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen. Formerly the Esperance Granite. Igneous rocks are metamorphosed to greenschist or amphibolite conditions; locally foliated or mylonitic. Strongly magnetic aerial images. Timing of intrusion is correlated with sinistral movement on the Mundrabilla Shear Zone and other late-stage faults in the Orogen. Various age determinations are given.|c.1200-1140 Ma.||||Widespread granitic rocks, undeformed to moderately deformed. Monzogranite, undeformed to moderately deformed, including magnetite-rich varieties, is mapped separately.|
78596|Esperance Supersuite|68654|5|Briefly described|p3|Mesoproterozoic|Mesoproterozoic|Albany-Fraser Orogen. Intrude Biranup and Nornalup Zones of the Kepa Kurl Booya Province.|1200-1140 Ma|||||
78596|Esperance Supersuite|69003|5|Briefly described|p4, p28, p44|||Nornalup Zone, Albany-Fraser Orogen.|c.1200-c.1140 Ma.||||Variably deformed (many with relatively undeformed interiors), strongly magnetic, voluminous granitic plutons.|
78596|Esperance Supersuite|69140|6|Mentioned|p2-3|Stenian|Stenian|Geological province: Albany-Fraser Orogen.|1200-1140 Ma|||||
78596|Esperance Supersuite|69252|5|Briefly described|p5, p7 Fig.3, p9, p15-16, p20-21, p24|Mesoproterozoic|Mesoproterozoic|See also p64-65, p72, p78, p80. Nornalup Zone, Albany-Fraser Orogen. Strongly magnetic plutons.|c.1200-1140 Ma (Spaggiari et al., 2011).|||Intrudes Recherche Supersuite and Mount Ragged Formation. Is intruded by Beenong Dyke Suite.|Granitic igneous rocks metamorphosed to greenschist and amphibolite facies; locally mylonitic.|
78596|Esperance Supersuite|69386|5|Briefly described|p4-6|Mesoproterozoic|Mesoproterozoic|Albany-Fraser Orogen.|1.20-1.14 Ga.||||Granitic rocks, typically unmetamorphosed; may include rocks metamorphosed up to greenschist or amphibolite grade.|
78596|Esperance Supersuite|69595|6|Mentioned|p3 fig 1, p4, p5, p14|Stenian|Ectasian|Albany-Fraser Orogen. Age of 1167 +/- 2 Ma is given for crystallisation of a granite from this supersuite.|c. 1200-1140 Ma||||Granites.|
78596|Esperance Supersuite|69632|5|Briefly described|p26|||May constitute basement in the Forrest Province beneath the Eucla Basin.|||||Granites.|
78596|Esperance Supersuite|69729|6|Mentioned|p88|Mesoproterozoic|Mesoproterozoic|Albany-Fraser Orogen.|c.1220-1120 Ma.|||||
78596|Esperance Supersuite|70023|5|Briefly described|p166-168,184|||Geological province: Albany-Fraser Orogen. Formed and intruded into Nornalup Zone  (Kirkland et al., 2011b, 2014; Spaggiari et al., 2011), and metamorphosed to greenschist and amphibolite facies (Myers, 1995; Nelson et al.,1995) during Stage II (c. 1225-1140 Ma) Albany-Fraser Orogeny.|1200-1140 Ma||||Granitic rock.|
78596|Esperance Supersuite|70084|4|Described|p219-220,222,229|Stenian|Stenian|Geological province: Albany-Fraser Orogen, Yilgarn Craton. Associated with Stage II (1225-1140 Ma) Albany-Fraser Orogen; immediately after emplacement of the Gnowangerup Fraser Dyke Suite (mafic magmatism ca. 1200 Ma). Mainly restricted to the Nornalup Zone and southeastern Biranup Zone and are geo-chemically distinct from all other granites of the Albany-Fraser Orogen. Similar in composition to the Pitjantjatjara Supersuite A-type granites and Moodini granite, however isotopically less radiogenic, indicating constrasnting basement composition. Reflects a significant change to higher crustal temperatures due to significant extension of dehydrated and refractory lower crust (probably associated with juvenile mantle input; Frost and Frost, 1997; Kilpatrick and Ellis, 1992; Smithies et al., 2011).|1200-1140 Ma|||||
78596|Esperance Supersuite|70085|6|Mentioned|p234|||Eastern Nornalup Zone, Albany-Fraser Orogeny.|1200-1140 Ma.|||||
78596|Esperance Supersuite|70089|6|Mentioned|p262, 264|Mesoproterozoic|Mesoproterozoic|Albany-Fraser Orogen.|1200-1140 Ma.|||||
78596|Esperance Supersuite|70090|6|Mentioned|p441-442,444-445|Stenian|Stenian|Geological province: Albany-Fraser Orogen, West Australian Craton. Felsic and mafic magmatism in the Biranup and Nornalup zones related to with Stage II (1225-1140 Ma) Albany-Fraser Orogen.|1200-1140 Ma|||||
78596|Esperance Supersuite|70153|5|Briefly described|500k_interpgeop14_lut.csv|Mesoproterozoic|Mesoproterozoic||1220 - 1100 Ma (inferred).||||Granite and monzogranite; undeformed to moderately deformed; includes magnetite-rich varieties.|
78596|Esperance Supersuite|70182|5|Briefly described|p2-4, p6-10, p13-15, p21, p33-34, p38|Mesoproterozoic|Mesoproterozoic|See also p45-47. Stage II of the Albany-Fraser Orogeny. Geochemistry diagrams.|1198 +/- 11 Ma - 1135 +/- 56 Ma.||Truslove, Booanya Suites.||Porphyritic granites.|
78596|Esperance Supersuite|70254|5|Briefly described|p357|Stenian|Stenian|Geological province: Biranup Zone, Albany-Fraser Orogen. Magmatism associated with Stage II (1215-1140 Ma) Albany-Fraser Orogen.|ca. 1140 Ma|||||
78596|Esperance Supersuite|70256|5|Briefly described|p2-3|Mesoproterozoic|Mesoproterozoic|Nornalup Zone, Albany-Fraser Orogen.|1200-1140 Ma.||||Granites.|
78596|Esperance Supersuite|70732|6|Mentioned|p284-285|Stenian|Stenian|Geological province: Albany-Fraser Orogen. Associated with Stage II (1225-1140 Ma) Albany-Fraser Orogeny.|1200-1140 Ma|||||
78596|Esperance Supersuite|70735|6|Mentioned|p28|||Albany-Fraser Orogen.|1200-1140 Ma.|||||
78596|Esperance Supersuite|70794|6|Mentioned|2_5m_interpgeop15_lut.csv|||||||Intrudes Recherche Supersuite.||
78596|Esperance Supersuite|70802|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage II (1225-1140 Ma). Generally lower in metamorphic grade, and less pervasively deformed, than those of the Recherche Supersuite. Locally exhibit magmatic fabrics and an overprinting weak to mylonitic foliation. Sample GSWA 182465 (metagabbro) yielded a concordia age of 1178+\-6 Ma, interpreted as the magmatic crystallization age of the gabbro. Sample GSWA 184374 (monzogranite) yielded a weighted mean 207Pb*/206Pb* date of 1198+\-11 Ma, interpreted as the magmatic crystallization age of the monzogranite. Sample GSWA 192586 (monzogranite) yielded a concordia age of 1175+\-12 Ma, interpreted as the magmatic crystallization age of the monzogranite. See 500k_interpgeop14_lut.csv, 250k_pre_mesozoic_interpgeop_lut.csv.|1220-1100 Ma (inferred)||Includes Booanya Suite, Truslove Suite.||Granitic rock; undeformed to moderately deformed|
78596|Esperance Supersuite|70813|5|Briefly described|p3, p5|Stenian|Stenian|Albany-Fraser Orogen.|c. 1200-1140 Ma||||Granitic rocks.|
78596|Esperance Supersuite|70826|6|Mentioned|p10|Mesoproterozoic|Mesoproterozoic|Albany-Fraser Orogen.|||||Granites|
78596|Esperance Supersuite|70831|5|Briefly described|p26|Stenian|Stenian|Albany-Fraser Orogen.|c. 1200-1140 Ma|||||
78596|Esperance Supersuite|71143|5|Briefly described|p433|||Geological province: Albany-Fraser Orogen. Similar age and composition to orthopyroxene- and pigeonite-bearing monzogabbro to monzodiorite rocks found from the Moodini Supersuite in the Madura Province.||||||
78596|Esperance Supersuite|71270|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen, West Australian Craton. Sample GSWA 182462 (metagabbro) yielded a weighted mean 238U/206Pb date of 1276+\-6 Ma, interpreted as the magmatic crystallisation age of the gabbro. See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv.|1198+\-11 Ma; 1140 Ma (inferred)||Includes Booanya Suite, Truslove Suite.|Locally forms net-veined complexes with Southern Hills Suite.|Granitic rock; undeformed to moderately deformed, typically porphyritic and locally with a magmatic foliation.|15-JUN-22
78596|Esperance Supersuite|71618|6|Mentioned|p135|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen. Associated with Stage II Albany-Fraser Orogen (Clark et al., 2000; Spaggiari et al., 2014). Possible, but unlikely source of c. 1150 (~1000-1300) Ma zircon in Shanes Dam Conglomerate.||||||
78596|Esperance Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Albany-Fraser Orogen. This unit also includes  at least two unnamed subunits.|Max age 1198+/-11 Ma, Min ~1140 Ma.||Includes Booanya Suite, Truslove Suite.|Locally forms net-veined complexes with Southern Hills Suite. May be included as intrusions in Recherche Supersuite units.|Granitic rock; undeformed to moderately deformed. Syenogranite; undeformed to moderately deformed; includes magnetite-rich varieties. Granitic rock, typically porphyritic and locally with a magmatic foliation;|
78596|Esperance Supersuite|72059|5|Briefly described|p56-57|Stenian|Stenian|Geological province: Fraser Zone, Albany-Fraser Orogen. Magmatism associated with Stage II (1225-1140 Ma) Albany-Fraser Orogeny.|1200-1140 Ma|||||
78596|Esperance Supersuite|72710|6|Mentioned|p4 Fig.2, p10.|Stenian|Stenian|Part of the Albany-Fraser Orogen.|1200 Ma to 1140 Ma.||Includes Booanya Suite.||Includes megacrystic monzogranite and syenogranite.|
78596|Esperance Supersuite|72934|6|Mentioned|p11|||Albany-Fraser Orogen.|||||May include A-type granite intrusions.|
78596|Esperance Supersuite|73084|6|Mentioned|p: 12, 21, 24, 54, 56, 66, 83, 124...|Stenian|Ectasia|Albany-Fraser Orogen. Similar in composition and age to the Moodini Supersuite and Pitjantjatjara Supersuite. Preserves an isotopic and geochemical heritage of reworked Archean crust of the Yilgarn Craton. Part of a regionally extensive, high-temperature event named the Maralinga Event by Spaggiari et al. (2016). Also p: 126, 131, 134, 139.|1200-1140 Ma, 1175 +/- 12 Ma||Booanya Suite, Connie Sue Formation.|||
78596|Esperance Supersuite|73480|6|Mentioned|p201 Fig.1, p206, p216|Stenian|Stenian|Includes the Burnside Batholith (ca 1180 Ma).|1200-1140 Ma|||||
78596|Esperance Supersuite|73597|6|Mentioned|p1178|Mesoproterozoic|Mesoproterozoic|Nornalup Zone, Albany-Fraser Orogen.|1200-1140 Ma.|||||
31770|Eurada Gneiss|23569|4|Described|p6 Tb. 1|Archean|Archean|Of the Narryer Terrane.   Monzogranitic to tonalitic gneiss with inclusions of Meeberrie Gneiss and Dugel Gneiss.  See also p5 Tb. 1.||||||07-NOV-08
31770|Eurada Gneiss|23574|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Dugel Gneiss. Underlying unit Meeberrie Gneiss.||||||07-NOV-08
31770|Eurada Gneiss|23576|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Dugel Gneiss. Underlying unit Meeberrie Gneiss.||||||07-NOV-08
31770|Eurada Gneiss|23577|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Dugel Gneiss. Underlying unit Meeberrie Gneiss.||||||07-NOV-08
31770|Eurada Gneiss|23781|4|Described|p15|Archean|Archean|||||||07-NOV-08
31770|Eurada Gneiss|24114|5|Briefly described|p5 Fig.4|Archean|Archean|Geological Province: Yilgarn Craton. Age: 3490-3440 Ma||||||07-NOV-08
31770|Eurada Gneiss|43835|5|Briefly described|Map Legend|Archean|Archean|Age about 3490-3480 & 3440Ma.||||||07-NOV-08
31770|Eurada Gneiss|50216|5|Briefly described|p203|Archean|Archean|Age: 3500-3400 Ma. Geological Province: Narryer Terrane in the northwestern part of Yilgarn Block.||||||07-NOV-08
31770|Eurada Gneiss|66299|4|Described|p28.|Archean|Archean|Narryer Terrane, Yilgarn Craton.|c.3500 to 3400 Ma.||||Tonalite and monzogranite gneiss.|
31770|Eurada Gneiss|67129|5|Briefly described|p4|Archean|Archean|Has not undergone granulite facies metamorphism, unlike the Meeberrie and Dugel Gneisses. Intruded by pegmatite or partially molten as indicated by younger zircon population of 3055 +/- 3 Ma.|3470-3440 Ma (SHRIMP U-Pb zircon).||||Tonalitic gneisses.|07-SEP-17
31770|Eurada Gneiss|68123|6|Mentioned|p30, 32, 35-37, 39|Archean|Archean|Narryer Terrane, Yilgarn Craton. Detrital zircons age peaks.|c.3490-3440 Ma.|||Intrudes Meeberrie Gneiss.||
31770|Eurada Gneiss|69583|5|Briefly described|p54|||Underwent deformation, and amphibolite to granulite facies metamorphism, at c.3300 Ma.||||Intrudes the Meeberrie Gneiss and Manfred Complex.|Felsic magma protolith.|
31770|Eurada Gneiss|70020|5|Briefly described|p116|Paleoarchean|Paleoarchean|Geological province: Yilgarn Craton. Felsic magmatic intrusion in the Meeberie Gneiss.|c. 3.3 Ga|||||
31770|Eurada Gneiss|71168|5|Briefly described|p6|Paleoarchean|Paleoarchean|Narryer and South West Terranes, Yilgarn Craton.|c. 3300 Ma|||Intrudes the Manfred Complex and the Meeberrie Gneiss.||
31770|Eurada Gneiss|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||felsic gneiss, granite|
31770|Eurada Gneiss|73526|5|Briefly described|p2 Fig.1, p3, p7|Paleoarchean|Paleoarchean|Narryer Terrane, central.|3490-3440 Ma||||Deformed tonalitic gneisses.|
27151|Euro Basalt|23416|5|Briefly described|Map Legend|Archean|Archean|Of Salgash Subgroup, Pilbara Craton||||||07-NOV-08
27151|Euro Basalt|23755|3|Fully described|p34|Archean|Archean|See also page 17 table 1. Of Warrawoona Group.||||||07-NOV-08
27151|Euro Basalt|23780|5|Briefly described|p133|Archean|Archean|||||||07-NOV-08
27151|Euro Basalt|23783|5|Briefly described|p15|Archean|Archean|Of Salgash Group.  Maximum thickness: 9400m.||||||07-NOV-08
27151|Euro Basalt|23807|6|Mentioned|p110 Fig. 2|||Geological Province: Pilbara Craton.||||||
27151|Euro Basalt|23813|5|Briefly described|p91 Tb. 1|Archean|Archean|Of the Warrawoona Group.  Age: c.3.48-3.43Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.||||||07-NOV-08
27151|Euro Basalt|24025|4|Described|p9 Tb. 1|Archean|Archean|Of Salgash Subgroup (Warrawoona Group).  Pillow basalt, tholeiitic basalt, chert, with perodotitic komatiite and high-Mg basalt. Max. thickness: 8000m. Geological Province: Pilbara Craton.||||||07-NOV-08
27151|Euro Basalt|24166|4|Described|p9|Archean|Archean|Of the Warrawoona Group.||||||07-NOV-08
27151|Euro Basalt|24184|4|Described|p701, 702|Archean|Archean|Of the Kelly Subgroup. Overlain by Wyman Formation. Geological Province: Pilbara Craton. Age: ca.3395-3325Ma. Now placed together with Wyman Formation in the newly defined Kelly Subgroup.||||||07-NOV-08
27151|Euro Basalt|24186|5|Briefly described|p776|Archean|Archean|Parent: Warrawoona Group||||||07-NOV-08
27151|Euro Basalt|24187|5|Briefly described|p776|Archean|Archean|Parent: Warrawoona Group||||||07-NOV-08
27151|Euro Basalt|24327|5|Briefly described|Map Legend|Archean|Archean|Fine to medium-grained mafic schist and amphibolite.  Of the Warrawoona Group. Age: <3475Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
27151|Euro Basalt|24349|5|Briefly described|Map legend|Archean|Archean|Of Warrawoona Group.   Age: <3475Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
27151|Euro Basalt|24531|4|Described|p17|Archean|Archean|Of Kelly Subgp. (Warrawoona Gp.). Conformably overlies Panorama Fm. Principally composed of interbedded, tholeiitic, high-Mg metabasalt and metadolerite, with thin beds of metamorphosed chert and quartzite. Max. thickness: 2.25m. In the Pilbara Craton.||||||07-NOV-08
27151|Euro Basalt|24532|5|Briefly described|Map legend|Archean|Archean|Of Salgash Subgroup (Warrawoona Group).  Geological Province: Pilbara Craton.||||||07-NOV-08
27151|Euro Basalt|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Formerly of Salgash Subgp - now assigned to newly formed Kelly Subgp. Includes Potkoorok, Miralga Creek + Cloisters Mbrs. Pillow basalts, pillow thol eiitic basalt, chert, komatiite, + high-Mg basalt. Overlies Panorama Fm. Max. thick: 9km. See p186-187.||||||07-FEB-11
27151|Euro Basalt|31309|2|Defined|p53|Archean|Archean|||||||07-NOV-08
27151|Euro Basalt|38498|5|Briefly described|Table 1|||||||||
27151|Euro Basalt|38544|6|Mentioned|Fig.1|||||||||
27151|Euro Basalt|39672|6|Mentioned|Fig.2|||||||||
27151|Euro Basalt|39697|3|Fully described|p95|||||||||
27151|Euro Basalt|40596|6|Mentioned|p67|||||||||
27151|Euro Basalt|41066|5|Briefly described|1 of 2 B01|||||||||
27151|Euro Basalt|41767|6|Mentioned|p45|||||||||
27151|Euro Basalt|43595|6|Mentioned|Table 2-28,p214|||||||||
27151|Euro Basalt|43698|6|Mentioned|p5|||||||||
27151|Euro Basalt|43769|6|Mentioned|Fig.3,p858|||||||||
27151|Euro Basalt|44150|5|Briefly described|p129 Tb.2-15,p132 Fig.2-131,p133 Tb.2-16|||See also p134, p139 Tb.2-18, p152 Tb.2-22, p157 Fig.2-144. 2 km thick. Formerly part of Empress Formation (of Fitton et al., 1975) and of Miralga Formation (Ingram, 1977). Similar to Apex Basalt except in east Pilbara where it is less mafic.||Salgash Subgroup|||Metamorphosed pillow basalt with minor chert and felsic volcanic units; local peridotitic komatiite near base.|
27151|Euro Basalt|44229|5|Briefly described|Map Legend|Archean|Archean|arc||||||07-NOV-08
27151|Euro Basalt|46922|6|Mentioned|p259|||Trace element analysis.||||||
27151|Euro Basalt|50189|4|Described|p9, 25|Archean|Archean|Uppermost part of the Salgash Subgroup. Metamorphosed, pillowed, tholeiitic and high-Mg basalts, komatiite. Unconformably overlain by Nimingarra Iron Formation, Fortescue Group; overlies Apex Basalt.||||||07-NOV-08
27151|Euro Basalt|50302|5|Briefly described|Map Legend|Archean|Archean|Of the Kelly Subgroup (Warrawoona Group).  Overlies: Strelley Pool Chert and Panorama Formation.  Underlies: Corboy Formation. Geological Province: Pilbara Craton.||||||07-NOV-08
27151|Euro Basalt|50379|5|Briefly described|Map Legend|Archean|Archean|Of Salgash Subgroup (Warrawoona Group). Geological Province: Pilbara Craton.||||||07-NOV-08
27151|Euro Basalt|50381|5|Briefly described|Map Legend|Archean|Archean|Of Kelly Subgroup (Warrawoona Group). Geological Province: Pilbara Craton.||||||07-NOV-08
27151|Euro Basalt|50423|4|Described|p216||Archean|Age: c. 3350. Komatiitic to basaltic volcanics. Base of upper Warrawoona Group.||||||07-NOV-08
27151|Euro Basalt|50427|4|Described|p185|Archean|Archean|Conformably overlies Strelley Pool Chert. 5-8km thick. Of upper Warrawoona Group.||||||07-NOV-08
27151|Euro Basalt|50430|4|Described|p160||Archean|Between 3420 and 3325 Ma. Up to 8km thick. Unconformably overlain by Sulphur Springs Group. In East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
27151|Euro Basalt|50544|3|Fully described|p23, p21 Tb. 4|Archean|Archean|At base of newly defined Kelly Subgroup (Warrawoona Group); previously was top unit of Salgash Subgroup. Unconformably overlain by Nimingarra Iron Fm (Gorge Creek Gp); disconformably overlies Panorama Fm. or Apex Basalt.  Max. thick:~3000m.||||||07-NOV-08
27151|Euro Basalt|50555|5|Briefly described|Map legend|Archean|Archean|Of the Kelly Subgroup (Warrawoona Group).  Basalt, pillow basalt, high-Mg basalt, and intercalated thin-bedded chert.  Geological Province: Pilbara Craton.||||||07-NOV-08
27151|Euro Basalt|60112|5|Briefly described|p108-112, p116.  |||Thickness to 5.5 km. 3395-3325 Ma (Van Kranendonk et al., 2002).|3395-3325 Ma|Unit in Warrawoona Group.||Overlies Strelley Pool Chert.|Maximum thickness 5.5km|
27151|Euro Basalt|60429|4|Described|p7, p12|Archean|Archean|Of Salgash Subgroup. Disconform.on Panorama Fm, or if absent, on Apex Basalt; unconform.overlain by Nimingarra Iron Fm. Intruded by Chimingadgi Trondhjemite+Mullugunya Granodiorite. Metamorphosed, pillowed tholeiitic+high-Mg basalts+perodotitic komatiite.||||||07-FEB-11
27151|Euro Basalt|60636|5|Briefly described|p37, p55|||Of the Warrawoona Group. Overlies Panorama Formation in the Kittys Gap area. Name used interchangeably with Euro Formation.||||||07-FEB-11
27151|Euro Basalt|61111|5|Briefly described|p97 Fig. 3, p100|||||||Overlies Panorama Formation|Komatiitic and tholeiitic basalt|
27151|Euro Basalt|61253|5|Briefly described|p51, p52 Fig. 2|Archean|Archean|Of the Kelly Group (Pilbara Supergroup). Now includes Six Mile Creek Formation (formerly of Sulphur Springs Group).  Geological Province:  Pilbara Craton.||||||07-NOV-08
27151|Euro Basalt|61256|5|Briefly described|p339|Archean|Archean|Unconformably overlain by Sulphur Springs Group rocks. Age: ca. 3.35Ga.  See also p340 Fig. 5a.||||||07-NOV-08
27151|Euro Basalt|61257|5|Briefly described|p354 Fig. 1|Archean|Archean|Ultramafic-mafic volcanic flows, with pillows.  Geological Province: North Pole Dome of the Pilbara Craton.  See also p355 Tb. 1.||||||07-NOV-08
27151|Euro Basalt|61264|5|Briefly described|p64 Fig. 2|||Of the Kelly Group (Pilbara Supergroup). Geological Province: East Pilbara Granite-Greenstone Terrane/Pilbara Craton.||||||17-MAY-06
27151|Euro Basalt|61266|4|Described|p56, p58 Tb.1|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group). Conformably overlies the Strelley Pool Chert. Geological Province: Pilbara Craton.||||||07-NOV-08
27151|Euro Basalt|61579|5|Briefly described|p58 Fig. 2|Archean|Archean|Of the Warrawoona Group.||||||07-NOV-08
27151|Euro Basalt|62427|5|Briefly described|p4, p6 Fig.3, p17-18 |Paleoarchean|Paleoarchean|See also Euro Formation. Age of deposition is constrained by the underlying and truncating units.|?3446 to 3415 Ma||||Silicified basalt and minor intercalated thin-bedded chert.|
27151|Euro Basalt|62979|5|Briefly described|p21 Fig. 1, p213 Fig. 2|Archean|Archean|Of the Kelly Group. Age: 3335-3325Ma. Geological Province: Pilbara Craton.||||||07-FEB-11
27151|Euro Basalt|63142|5|Briefly described|p487 Fig. 2|||Geological Province: Warrawoona Syncline.||||||
27151|Euro Basalt|63245|5|Briefly described|p5 Fig. 2|Archean|Archean|Of the Kelly Group (Pilbara Supergroup). Age: ~3350Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
27151|Euro Basalt|63417|5|Briefly described|Map legend|Archean|Archean|Of the Kelly Group (Pilbara Supergroup). Age: 3350Ma. Geological Province: Pilbara Craton. Basalt, komatiitic basalt and serpentinised peridotite; local dolerite and gabbro sills; minor felsic volcaniclastic rocks and chert; metamorphosed.||||||04-DEC-08
27151|Euro Basalt|63420|5|Briefly described|Map legend|Archean|Archean|Of Kelly Gp (Pilbara Supergp). Geol.Prov: Pilbara Craton. Basalt, komatiitic basalt and serpentinised peridotite; local dolerite sills;minor felsic volcaniclastic rock and chert; metamorphosed komatiitic basalt, massive and pillowed lavas.................||||||07-NOV-08
27151|Euro Basalt|63441|5|Briefly described|p4 Tb. 1, p20|Archean|Archean|Of the Kelly Group (Pilbara Supergroup). Now includes rocks formerly assigned to the briefly used Copper Gorge Formation, over which the basalt conformably lay.||||||07-FEB-11
27151|Euro Basalt|63538|4|Described|p3 Fig. 2, p5, p8 Tb. 1, p9-10, p11|Archean|Archean|Of Kelly Group. Underlain conformably by Strelley Pool Chert. Overlain by Wyman Formation. Age: 3350-3315 Ma. Thick: ~6500m. Geological Province: Pilbara Craton. Komatiitic and tholeiitic basalts. See p10 for more information.||||||19-APR-13
27151|Euro Basalt|63649|5|Briefly described|p201|Archean|Archean|Of the Kelly Group. Age: 3.363 - 3.346Ga. Geological Province: Pilbara Craton.||||||07-FEB-11
27151|Euro Basalt|63854|5|Briefly described|p229 Fig.2 |||||Of the Kelly Group.||||
27151|Euro Basalt|64326|6|Mentioned|p72|Archean|Archean|Thickness range: 5-9km.||||||07-FEB-11
27151|Euro Basalt|64328|5|Briefly described|p54, p57 Tb. 2|Archean|Archean|Of Kelly Subgroup (Warrawoona Group). Formerly part of Salgash Subgroup but recent intepretations of its volcanic origins have caused its separation and removal to the Kelly Subgroup above. Age: 3420-3325Ma. Tholeiitic pillow basalt mainly; some chert.||||||07-FEB-11
27151|Euro Basalt|64405|5|Briefly described|p1, p8, p15-16, p17|Archean|Archean|Of the Kelly Group (Pilbara Supergroup). Overlies Strelley Pool Formation, conformably or disconformably. Age: 3350-3315Ma. Geological province: East Pilbara Terrane. Komatiitic basalt.||||||07-FEB-11
27151|Euro Basalt|64621|5|Briefly described|Map legend|Archean|Archean|Of the Kelly Group (Pilbara Supergroup). Age: c.3350Ma. Basalt, komatiitic basalt and serpentinised peridotite; local dolerite sills; minor felsic volcaniclcastic rocks and chert; metamorphosed.||||||04-DEC-08
27151|Euro Basalt|64628|6|Mentioned|p171 Fig.1. |||Coppin Gap greenstone belt, Pilbara Craton.||||||
27151|Euro Basalt|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Kelly Subgroup. Geological Province: Pilbara Craton. Basalt; generally pillowed; minor komatiitic basalt; metamorphosed. Chert and dolerite and gabbro also present in the unit.||||||07-FEB-11
27151|Euro Basalt|64654|5|Briefly described|Map Legend|Archaean|Archaean|Of Kelly Group.  Age: 3350-3335Ma. Geological Province: Pilbara Craton. Basaltic volcanic rocks, komatiitic basalt, chlorite schist, massive dolerite and gabbro basalt and chert; metamorphosed.||||||17-NOV-08
27151|Euro Basalt|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Kelly Group. Age: 3350-3335Ma. Geological Province: Pilbara Craton. Medium-grained amphibolite and amphibolite schist; derived from basaltic volcanic rocks, chert and basalt.||||||26-NOV-08
27151|Euro Basalt|64747|6|Mentioned|p94 fig 1, p95 fig 2|||||Unit in Kelly Group.||||
27151|Euro Basalt|64936|5|Briefly described|map legend|Archean|Archean|Of Kelly Subgroup. Age: c. 3350-3335 Ma (geochron: DR Nelson in prep). Tholeiitic basalt; metakomatiite; chert; sandstone and siltstone. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
27151|Euro Basalt|65008|4|Described|p5, p7-12, p20, p21, p26-29, p41|Archean|Archean|East Pilbara Granite-Greenstone Terrane. Includes 9 separately mapped facies. Redefined by Bagas et al. (2004a) as included in the Kelly Subgroup. ~5km thick. Hosts Cu-Mo-W(-F) deposits and occurrences.|3250-3325 Ma|Of the Kelly Subgroup||Intruded by the Boobina Porphyry. Conformably underlain by the Strelley Pool Chert. Conformably overlain by the Wyman Formation.|Basalt; generally pillowed; minor komatiitic basalt; medium-grained dolerite and local gabbro; chert; generally white, grey, and blue-black layered chert; local massive blue-grey chert. All metamorphosed to weakly metamorphosed.|
27151|Euro Basalt|65724|5|Briefly described|map legend|Paleoarchaean|Paleoarchaean|Of Kelly Group. Unconformable under Mount Roe Basalt; intruded by Elsie Creek Tonalite. Mafic and psammopelitic schist; pelite; basalt; komatiitic basalt; chert. Age: c. 3350Ma (geochron. Nelson in prep) Geol.Prov: East Pilbara Granite-Greenstone Terrane||||||
27151|Euro Basalt|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton. Mapped as five sub-units.||Of Kelly Subgroup.|||Undivided metamorphosed mafic volcanic rock and sedimentary rock; basalt, mostly pillowed; minor massive dolerite, gabbro and komatiitic basalt; white, grey, and blue-black banded chert; hydrothermal black chert vein.|
27151|Euro Basalt|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Mapped as six sub-units.||Of Kelly Group.|||Basalt, komatiitic basalt, serpentinized peridotite, local dolerite sills, minor felsic volcaniclastic rocks, metamorphosed; silicified meta-ultramafic volcanic rock; pillowed basalt; chert, layered and locally massive; hydrothermal chert in veins.|
27151|Euro Basalt|65757|6|Mentioned|p87|||Pilbara Craton||||||
27151|Euro Basalt|65825|3|Fully described|p6, p7 Fig.4, p32.|Archean|Archean|14 un-named sub-units with differing lithologies are mapped separately and described in detail in the report. Re-assigned by Van Kranendonk et al. (2004) to the Kelly Group. Thickness to 9 km inferred. Depositional age of c.3395 - 3325 Ma interpreted by Van Kranendonk et al. (2002).|>3325 Ma.|Unit in Kelly Group; formerly in Warrawoona Group.||Is intruded by granites of Yilgalong Granitic Complex. Is overlain paraconformably by Wyman Formation or unconformably by Fortescue Group.|Metamorphosed komatiitic basalt constitutes 60-70% of the succession: grey-green, locally abundant varioles, spinifex texture, pillows; mafic schist; subordinate fine-grained gabbro, chert, ultramafic rocks, and clastic sedimentary rocks.|
27151|Euro Basalt|65827|3|Fully described|p6 Tb.1, p12 Tb.3, p16, p21, p28-29|Paleoarchean|Paleoarchean|Of Kelly Group; formerly of Kelly Subgroup. c.3350-3325 Ma. Underlies Wyman Fm conformably; unconformably underlies Gorge Creek Gp, Fortescue Gp, Farrel Quartzite; conformably overlies Strelley Pool Chert; disconformably overlies Panorama Fm. Intruded by Gobbos Granodiorite, Dalton Suite. Voluminous (up to 9 km thick), metamorphosed, pillowed mafic-ultramafic lavas; bands of chert.||||||
27151|Euro Basalt|65828|5|Briefly described|Map legend|Archean|Archean|||Unit in Kelly Subgroup.|||Basalt, generally pillowed; metamorphosed; minor komatiitic basalt, carbonate-altered and silicified basalts; mafic schist, slate and strongly foliated komatiitic basalt.|
27151|Euro Basalt|65829|3|Fully described|p7 Fig.3, pp9-11, p13, p32, p34.|Paleoarchean|Paleoarchean|Voluminous eruption of mafic-ultramafic lavas in the Mount Elsie greenstone belt; attributed to mantle plume activity. Overall dips steeply to moderately west and northwest, away from Yilgalong Granitic Complex. Local occurrences of partly silicified sheets of dissected, secondary carbonate or residual calcrete. Has been explored for gold at Elsie Creek.|3350 - 3325 Ma.|Unit in Kelly Group.||Is intruded by Elsie Creek Tonalite and Yilgalong Granitic Complex. Is overlain conformably by Wyman Formation, and unconformably by Mount Roe Basalt.|Mafic schists derived from komatiitic and tholeiitic basalts; metamorphosed green-grey fine-grained komatiitic basalt; red-brown ferruginised and silicified psammopelitic schist; fine-grained quartz-chlorite pelite; pillowed tholeiitic basalt.|
27151|Euro Basalt|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Kelly Group. Age shown as 3350-3335 Ma. Basalt, komatiitic basalt, serpentinized peridotite; local dolerite and gabbro sills; minor felsic volcaniclastic rocks and chert; metamorphosed.||||||11-APR-13
27151|Euro Basalt|66122|5|Briefly described|p75|Archean|Archean|Mount Goldsworthy greenstone belt, NE Pilbara Craton.||Warrawoona Group.|||Tholeiitic and komatiitic basalt, mafic schist, dolerite sills.|
27151|Euro Basalt|66217|4|Described|p5, p14, pp28-30, p59.|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Van Kranendonk et al. (2002) included this unit in the Kelly Subgroup in their redefinition of the Warrawoona Group. Thickness to 9400 m.|3350-3325 Ma.|Unit in Kelly Group.||Conformably overlies Strelley Pool Formation. Is overlain conformably by Wyman Formation.|Thick volcanic succession of interbedded basalt, komatiitic basalt and komatiite; several thin, silicified interflow sedimentary units; minor felsic, tuffaceous sandstone.|
27151|Euro Basalt|66664|5|Briefly described|p6, p7, p8. |||||Unit in Kelly Group.|||Mainly tholeiitic pillow basalt; minor chert.|
27151|Euro Basalt|66745|4|Described|p55, p57.|Paleoarchean|Paleoarchean|Genetically related to upper part of Strelley Pool Formation. Major deepening of depositional basins, with many kilometres of deep-water volcanics overlying the Strelley Pool Formation unconformity.|3350-3335 Ma.|Basal unit in Kelly Group.||Locally overlies Warrawoona Group. Elsewhere, paraconformably overlies Strelley Pool Formation. Is overlain by Wyman Formation.|Basalt, komatiitic basalt, komatiite; minor felsic volcanic rocks.|
27151|Euro Basalt|67130|5|Briefly described|p16, p20, p61, p63, p76|Paleoarchean|Paleoarchean|Komatiite up to 1.5km thick and tholeiitic basalt and komatiitic basalt up to 5km thick, erupted over 25 Ma.|3350 Ma - 3320 Ma|Kelly Group||Conformably overlies Strelley Pool Formation, overlain by Wyman Formation|High Mg tholeiitic basalt, chert, komatiiite and komatiitic basalt.|
27151|Euro Basalt|67197|5|Briefly described|p2, p4-9, p13-14, p18-19, p22, p25, p29|Paleoarchean|Paleoarchean|See also p33-34, p36, p52, p62. Pilbara Craton.|3350-3325 Ma.|Kelly Group.||Unconformably overlies Strelley Pool Formation.|Pillow basalt; includes bedded chert.|
27151|Euro Basalt|67201|4|Described|p7 Fig.4, p12 Tb.1, p24|||In northern Pilbara Craton, East Pilbara Terrane.|c. 3350 Ma|Kelly Group||||
27151|Euro Basalt|67269|5|Briefly described|p3, p6-7 Figs.3-4, p9, p12, p14, p26|Paleoarchean|Paleoarchean||3350-3335 Ma.|Kelly Group.||Overlies Strelley Pool Formation. Is overlain by Wyman Formation or unconformably by Leilira Formation.|Mainly tholeiitic pillow basalt; basaltic komatiite, pillowed; komatiite, in flows and intrusions.|
27151|Euro Basalt|67270|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.|3350-3335 Ma.|Kelly Group.||||
27151|Euro Basalt|67668|5|Briefly described|Fig. 2-4; p. 154, 157,; Tb.1.  ||Paleoarchean|East Pilbara Terrane, Pilbara Craton. 5-8 km thick. Possible evidence of early life is reviewed. |3350 - 3325 Ma|Kelly Group||Underlies the Wyman Formation, overlies the Strelley Pool Formation.|Sequence of tholeiitic, komatiitic and high-magnesium basalt, often pillowed, with numerous thin (<10 m) inter-beds of chert and volcaniclastics.|
27151|Euro Basalt|68035|4|Described|p288 Fig 4|Paleoarchean|Paleoarchean|Pilbara Supergroup, East Pilbara Terrane.|3350 - 3335 Ma|Of Kelly Group.||Paraconformably overlies Strelley Pool Formation. Overlain by Wyman Formation.|Basalt, komatiitic basalt, felsic volcanics, komatiite.|
27151|Euro Basalt|68280|5|Briefly described|p4, p6, p20||||3350-3335 Ma|Kelly Group||Overlain by Wyman Formation, overlies Strelley Pool Formation|Tholeiitic basalt, komatiite, komatiitic basalt, chert and felsic volcanic rocks. 9.44km thick.|16-JAN-23
27151|Euro Basalt|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Detailed lithology discussed in map legend; the 13 facies are mapped separately.|3350-3335 Ma|Of the Kelly Group.|||Basalts: komatiitic, massive, pillowed; dolerite; felsic volcaniclastic rock; felsic volcanic sandstone; chert; quartz-rich sandstone; grey sandstone; hydrothermal chert; schists: strongly sheared chlorite, mafic, tremolite-chlorite-serpentinite.|
27151|Euro Basalt|68282|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. 18 facies are mapped separately.|3350-3335 Ma|Of the Kelly Group|||Chlorite schist; amphibolite and metabasalt; silicified and sericitised metabasalt; mafic schists; serpentinized peridotite and komatiite; quartz-rich sandstone; chert veins; banded iron-formation; basalt: komatiitic, massive, pillowed; dolerite.|
27151|Euro Basalt|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Includes 1 unnamed subunit.|c.3350-3335 Ma|Of the Kelly Group.|||Basalt, komatiitic basalt, and serpentinized peridotite, local dolerite sills, minor felsic volcaniclastic rock and chert; komatiitic basalt, massive and pillowed lavas and subvolcanic intrusions, local pyroxene spinifex texture; all metamorphosed.|23-SEP-13
27151|Euro Basalt|68284|5|Briefly described|p4, 6-10, 15|Paleoarchean|Paleoarchean|Crops out in the Marble Bar-Nullagine area, East Pilbara Terrane. 4km (locally up to 9km) thick.|3350-3325 Ma.|Kelly Group.||Disconformably to paraconformably overlies Strelley Pool Formation. Is overlain conformably by Wyman Formation.|A thick, mainly basaltic succession also containing komatiite, komatiitic basalt, numerous thin chert units, and local clastic and volcaniclastic sedimentary rocks. Many pillow basalt units. All metamorphosed to greenschist facies.|
27151|Euro Basalt|69012|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane. Nineteen facies [!!] are mapped separately.|3350-3335 Ma|Of the Kelly Group.|||Basalt: pillowed, komatiitic, carbonate-altered and massive; basaltic and felsic volcaniclastic rocks; dolerite and local gabbro; altered ultramafic rock; amphibolite, metabasalt and mafic schist; metamorphosed chert; hydrothermal chert in veins.|29-APR-14
27151|Euro Basalt|69013|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|See map legend for a detailed lithological description. Mapped as 14 facies.|3350-3335 Ma|Of the Kelly Group.|||Metabasalt, mafic schist, chert, basalt.|30-APR-14
27151|Euro Basalt|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Mapped as 13 separate unnamed units. See map legend for a detailed lithological description.|3350-3335 Ma|Of the Kelly Group.|||Includes chlorite schist; carbonate altered mafic volcanic rock; tremolite-chlorite-serpentine schist; chert; sandstone, siltstone, and shale; massive, pillowed, and komatiitic basalt; pyroxene leucogabbro; dolerite.|02-MAY-14
27151|Euro Basalt|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Psammopelitic schist, metachert, chlorite schist,paragneiss, metapyroxenite, metaperidotite, mafic and ultramafic schist. Sandstone, siltstone, and shale.Age derived from quartzite and volcanigenic sandstone samples (168999.1.pdf, 178042.1.pdf) |3335 Ma +/-7 Ma - 3350 +/- 3 Ma (SHRIMP)|Kelly Group|||Basalt, komatiitic basalt,komatiite, amphibolite, metabasalt, serpentinized peridotite; local dolerite and gabbro sills; Felsic volcaniclastic rocks and chert; metamorphosed. Pelite interbedded with chert and fine grained tuffaceous rocks.|
27151|Euro Basalt|69301|4|Described|p5 Fig.3, p9 Tb.1, p10-11|||Pilbara Craton. East Pilbara Terrane. Thickness: up to 400 m.|3350-3335 Ma; 3350 Ma|Kelly Group|||Basalt; with komatiitic basalt.|
27151|Euro Basalt|69566|5|Briefly described|p236-237|||East Pilbara Granite-Greenstone Terrane.||Kelly Group.||Overlies Panorama Formation (Warrawoona Group). Is overlain by Wyman Formation.|Interbedded komatiitic and tholeiitic basalts.|
27151|Euro Basalt|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA 168999 (recrystallised quartzite) yielded an interpreted maximum depositional age of 3335+\-7 Ma for the sandstone protolith (weighted mean 207pb/206Pb). Sample GSWA 178007 (feldspar-quartz porphyry) yielded an interpreted igneous crystallisation age of 3279+\-4 Ma for the porphry (weighted mean 207pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 250k_interpgeol_lut.csv.|3350-3325 Ma|Unit of Kelly Group.||Overlain by Kangaroo Caves Formation. Intruded by Gobbos Granodiorite.|Amphibolite, basalt; komatiitic; dolerite, chert and hydrothermal chert, sandstone, siltstone shale, quartzite, felsic, mafic and ultramafic extrusive rocks, metaperidotite, metapyroxenite, serpentinite, dunite, schist.|
27151|Euro Basalt|70022|6|Mentioned|p115|||East Pilbara Terrane.||Kelly Group.||||
27151|Euro Basalt|70507|5|Briefly described|p431|Archean|Archean|Geological province: Pilbara Craton.||Unit of Kelly Group.||||
27151|Euro Basalt|70775|5|Briefly described|p12, p80|Paleoarchean|Paleoarchean|East Pilbara.|c. 3350 Ma|Kelly Group||Disconformably overlies the Strelley Pool Formation. Overlain by the Wyman Formation.||
27151|Euro Basalt|70834|6|Mentioned|p298|Paleoarchean|Paleoarchean|Marble Bar greenstone belt, Pilbara Craton.||||Overlies Strelley Pool Formation. Is overlain unconformably by Gorge Creek Group.|Basalt, komatiite.|
27151|Euro Basalt|70884|5|Briefly described|p123-124,135|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|~3.33 Ga|Unit of Kelly Group.||Overlain by Wyman Formation. Underlain unconformably by Strelley Pool Formation.||
27151|Euro Basalt|71041|5|Briefly described|p44|Paleoarchean|Paleoarchean|Basalts and BIFs have been reassigned to the Honeyeater Basalt. |3340 Ma|||||
27151|Euro Basalt|71267|6|Mentioned|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||basalt, chert, dolerite, gabbro|
27151|Euro Basalt|71487|5|Briefly described|p127,139|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|3350 Ma|Unit of Kelly Group.||Underlain conformably by Strelley Pool Formation.||
27151|Euro Basalt|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Kelly Large Igneous Province, East Pilbara Terrane.|Max age 3350+/-3 Ma, min3335+/-7 Ma.|Kelly Group|||Basalt, komatiitic basalt, serpentinized peridotite; local dolerite and gabbro sills; minor felsic volcaniclastic rocks and chert; metamorphosed.|
27151|Euro Basalt|72064|5|Briefly described|p66-67|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|c. 3350-3335 Ma|Unit of Kelly Group.||Lowermost unit of Kelly Group. Overlain by Wyman Formation. Underlain paraconformably by Strelley Pool Formation.||
27151|Euro Basalt|72251|5|Briefly described|p54|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Kelly Group.||Lowermost unit of Kelly Group. Overlain by Wyman Formation. Underlain by Strelley Pool Formation.||
27151|Euro Basalt|72668|5|Briefly described|p4-6, p8, p19, p26|||East Pilbara Terrane.  ~5km thick.|3350-3320 Ma|Kelly Group||Overlies the Strelley Pool Chert conformably. Overlain by the Wyman Formation.|Basal komatiite overlain by komatiitic basalt and tholeiitic basalt.|13-JAN-22
27151|Euro Basalt|73160|6|Mentioned|p2 Fig.1|||Pilbara Craton.||Kelly Group||||
27151|Euro Basalt|73598|5|Briefly described|p1208-1209, 1211-1212|Paleoarchean|Paleoarchean|East Pilbara Terrane. The thickest basaltic formation in the Pilbara Terrane. Fed by Kelly Dyke swarm dykes. REE diagrams. Suggested link with Kromberg Formation (Kaapvaal craton) based on geochronology and lithology implies an areal extent of >1,000,000 km2.|3317 Ma.|Kelly Group.||Overlies Strelley Pool Formation. Is overlain by Wyman Formation.|Widespread komatiitic pillow basalts (c.1.5 km thick) overlain by c.5 km of komatiitic and tholeiitic basalt.|
79352|Evaporation Monzogranite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|3010-2600 Ma (inferred)||||Metamonzogranite; foliated to gneissic, and equigranular to sparsely porphyritic|
80954|Famennian reef complexes, marginal slope and basin facies 80954|72034|5|Briefly described|500k_interpgeop16_lut|Famennian|Famennian|Unnamed informal unnamed unit. Lennard Shelf, Canning Basin. Age: biostratigraphic.|||||Limestone, calcareous sandstone and mudstone; lesser siliciclastic sandstone and conglomerate.|
80955|Famennian reef complexes, platform facies 80955|72034|5|Briefly described|500k_interpgeop16_lut|Famennian|Famennian|Unnamed informal unit. Lennard Shelf, Canning Basin. Age: biostratigraphic. Includes Windjana and Nullara Limestones.|||||Limestone, lesser sandstone and siltstone, bedded (backreef) to massive (reef).|
25905|Fargoo Tillite|14019|5|Briefly described|p16, 19|||Of the Duerdin Group. Unconformably overlies: Angalarri Siltstone. Geological Province: Wolfe Creek Basin. Correlated with Olympic Formation. Possibly equivalent to diamictite of the Duerdin Group.||||||
25905|Fargoo Tillite|23314|6|Mentioned|334|||||||||
25905|Fargoo Tillite|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|Of Duerdin Group.||||||
25905|Fargoo Tillite|28255|3|Fully described|p71, Tb. 11(opp.p8)|Adelaidean|Adelaidean|Of the Duerdin Group. Tillite and dolomitic conglomerate. Conformably overlies, and intertongues with, Skinner Sandstone; unconformably overlain by Blackfellow Creek Sandstone (AUVERGNE sheet).  Max. thickness: >20m.||||||18-SEP-06
25905|Fargoo Tillite|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
25905|Fargoo Tillite|31645|6|Mentioned|Table 2|||Correlation||||||
25905|Fargoo Tillite|32660|5|Briefly described|Table 6|||||||||
25905|Fargoo Tillite|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Duerdin Group.  Tillite, dolomite clasts common.||||||02-DEC-04
25905|Fargoo Tillite|32701|4|Described|Table 1|||Adelaidean. Duerdin Gp. See p14.||||||18-SEP-06
25905|Fargoo Tillite|32728|6|Mentioned|Table 7|||See also Fig.16||||||
25905|Fargoo Tillite|33375|6|Mentioned|p11 Tb. 1, p13|Adelaidean|Adelaidean|Of the Duerdin Group. Tillite, dolomite conglomerate lenses. Intertongues with Skinner Sandstone in east; unconformable on Angalarri Siltstone farther west.||||||26-APR-05
25905|Fargoo Tillite|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
25905|Fargoo Tillite|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Duerdin Group. Tillite, dolomite, conglomerate.||||||27-APR-05
25905|Fargoo Tillite|36888|4|Described|p215|||||||||
25905|Fargoo Tillite|36898|6|Mentioned|p181|||||||||
25905|Fargoo Tillite|37462|5|Briefly described|p293|||||||||
25905|Fargoo Tillite|37927|4|Described|p504|||||||||
25905|Fargoo Tillite|38157|6|Mentioned|Table X|||||||||
25905|Fargoo Tillite|39210|5|Briefly described|Fig.18|||||||||
25905|Fargoo Tillite|41405|5|Briefly described|p206|||||||||
25905|Fargoo Tillite|43855|5|Briefly described|Map Legend||Proterozoic|||||||
25905|Fargoo Tillite|44140|5|Briefly described|p300, p301 fig 4-7, p303 Tb. 4-2|Neoproterozoic|Neoproterozoic|Of East Kimberley area. Correlated with Marinoan glaciation (670 Ma). Up to 200 m thick.||Duerdin Group||Overlain conformably by Frank River Sandstone.|Tillite with large lenses of boulder conglomerate.|07-MAR-18
25905|Fargoo Tillite|44317|4|Described|Table 3||Adelaidean|||||||
25905|Fargoo Tillite|44318|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
25905|Fargoo Tillite|44868|5|Briefly described|Map Legend||Phanerozoic|||||||
25905|Fargoo Tillite|45041|6|Mentioned|p45|||Refers Dow & Gemuts (1969)||||||
25905|Fargoo Tillite|45047|2|Defined|p82|Adelaidean|Adelaidean|See also pp83,36,38,40.||||||18-SEP-06
25905|Fargoo Tillite|45112|4|Described|p39|||p39.||||||18-SEP-06
25905|Fargoo Tillite|48927|6|Mentioned|Table 1|||Refers Dow & Gemuts (1969)||||||
25905|Fargoo Tillite|48938|4|Described|p65|||See also pp66-67. Section p98.||||||18-SEP-06
25905|Fargoo Tillite|48943|3|Fully described|p80|||||||||
25905|Fargoo Tillite|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Wolfe Creek Basin. Of Duerdin Group. Unconformably overlies Skinner Sandstone. Overlain by Blackfellow Creek Sandstone. Diamictite, abundant dolostone clasts.||||||21-JUL-04
25905|Fargoo Tillite|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Duerdin Group. Geological Province: Wolfe Creek Basin. Matrix-supported, polymictic pebble-boulder conglomerate, and sandstone; clasts in conglomerate are polished and striated locally.||||||
25905|Fargoo Tillite|60682|4|Described|p17 Table 4, 18|Neoproterozoic|Neoproterozoic|Of Duerdin Group. Conformably overlies Skinner Sandstone. Unconformably overlain by Blackfellow Creek Sandstone. Max. thickness: >100m. Geological Province: Wolfe Creek Basin.||||||
25905|Fargoo Tillite|63458|6|Mentioned|p872-889, p891, p893, p896-897, p900. |Cryogenian|Cryogenian|East Kimberley region. Overlies striated pavement.||Unit in Duerdin Group.||Correlated with Olympic Formation. Is overlain by Frank River Sandstone.|Diamictite and conglomerate.|
25905|Fargoo Tillite|63762|5|Briefly described|p19|||See also Fargoo Formation.||||||07-FEB-11
25905|Fargoo Tillite|64104|6|Mentioned|p63|Neoproterozoic|Neoproterozoic|The author proposes this name be replaced by Fargoo Formation "to distinguish stratigraphic terms from genetic interpretation". Whatever; see references to Fargoo Formation throughout the article.||||||
25905|Fargoo Tillite|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic |Of Duerdin Group, Wolfe Creek Basin. Diamictite, abundant dolostone clasts||||||
25905|Fargoo Tillite|67151|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Wolfe Basin.||Unit in Duerdin Group.||Overlies Skinner Sandstone. Is unconformably overlain by Blackfellow Creek Sandstone.|Diamictite with locally abundant dolostone clasts, dolostone, conglomerate.|
25905|Fargoo Tillite|67484|6|Mentioned|p295 Fig.2|Cryogenian|Cryogenian|More commonly referred to as the Fargoo Formation in the Text.||Of the Duerdin Group.||||
25905|Fargoo Tillite|68244|6|Mentioned|p667|Neoproterozoic|Neoproterozoic|See Fargoo Formation.||||||
25905|Fargoo Tillite|68277|6|Mentioned|p95|Neoproterozoic|Neoproterozoic|The rank is not given in the text.||||||
25905|Fargoo Tillite|68473|6|Mentioned|p531-532|||Adelaide Rift Complex.||Duerdin Group||||
25905|Fargoo Tillite|68733|6|Mentioned|p177 Fig.2, p188, p189 Fig.8|Cryogenian|Cryogenian|Victoria and Wolfe basin.||Of the Duerdin Group.|||Glacigenic sediments.|05-DEC-17
25905|Fargoo Tillite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Wolfe Creek Basin||Duerdin Group|||Massive, matrix-supported, polymictic pebble to boulder conglomerate and poorly sorted massive sandstone; larger clasts in conglomerate are polished and striated locally.|31-JUL-15
25905|Fargoo Tillite|69165|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|||Duerdin Group|||Massive, matrix supported, polymictic pebble to boulder conglomerate and poorly sorted massive sandstone; larger clasts in conglomerate are polished and striated locally.|
25905|Fargoo Tillite|69418|6|Mentioned|p3:31|||Wolfe Basin. Hosts barite at the Newry deposit (briefly described).||||||12-JUL-16
25905|Fargoo Tillite|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Ediacaran|Victoria/Wolfe Basins, Centralian A Superbasin. Supersequence 3.||Duerdin Group.||Overlies Skinner Sandstone. Is overlain by Blackfellow Creek Sandstone.||12-JUL-16
25905|Fargoo Tillite|69442|5|Briefly described|p27:1-4, 6-7|||Wolfe Basin. Over 100m thick. Glacial deposits. Low-angle unconformity at the top. Hosts a small uneconomic vein of barite in a minor fault at the Newry prospect.||Duerdin Group.||Conformably overlies Skinner Sandstone. Is overlain unconformably by Blackfellow Creek Sandstone. Correlated with Olympic Formation (Amadeus Basin).|Diamictite: characterised by a predominance of dolostone boulders, some of which are stromatolitic; many have a foetid odour when broken.|12-JUL-16
25905|Fargoo Tillite|69634|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1.|635-541 Ma (Inferred)|Unit of Duerdin Group.|||Massive, matrix-supported, polymictic pebble to boulder conglomerate and poorly sorted massive sandstone; larger clasts in conglomerate are polished and striated locally|
25905|Fargoo Tillite|69673|5|Briefly described|p190|Neoproterozoic|Neoproterozoic|More than 100m thick.||Duerdin Group|||Tillite with dolostone boulders.|
25905|Fargoo Tillite|70154|4|Described|100k_interpgeop_lut.csv|Ediacaran|Cryogenian||541-850 Ma|Duerdin Group|||Massive matrix supported polymictic pebble to boulder conglomerate and poorly sorted massive sandstone.|
25905|Fargoo Tillite|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin. ||Duerdin Group|||Diamictite, abundant dolostone clasts.|
25905|Fargoo Tillite|70655|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin.||Duerdin Group.||Shown as overlying Skinner Sandstone, and overlain by Blackfellow Creek Sandstone, unconformably.|Diamictite with locally abundant dolostone clasts, dolostone, conglomerate.|
25905|Fargoo Tillite|71267|4|Described|GEOL_LUT_CSV files|Cryogenian|Cryogenian|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv.|720-635 Ma (inferred)|Unit of Duerdin Group.|||Massive, matrix-supported, polymictic pebble to boulder conglomerate and poorly sorted massive sandstone; larger clasts in conglomerate are polished and striated locally|
25905|Fargoo Tillite|73255|6|Mentioned|p534 Fig.2, p548 Fig.12|Cryogenian|Cryogenian|||Duerdin Group||Disconformably overlies the Helicopter Siltstone, underlies the Frank River Sandstone.||
70125|Farrel Quartzite|63417|5|Briefly described|Map legend|Archean|Archean|Of the Gorge Creek Group (De Grey Supergroup).  Age: c. 3020Ma. Geological Province: Pilbara Craton. Quartz sandstone and quartzite; locally fuchsitic; minor conglomerate and chert; metamorphosed.||||||07-NOV-08
70125|Farrel Quartzite|63420|5|Briefly described|Map legend|Archean|Archean|Of Gorge Creek Group (De Grey Supergroup). Geological Province: Gorge Creek Basin/ Pilbara Craton. Quartz sandstone; local basal polymictic conglomerate and siltstone; silicified; metamorphosed.||||||07-NOV-08
70125|Farrel Quartzite|63441|2|Defined|p5 Tb.1, p26|Archean|Archean|Basal unit of Gorge Creek Gp (Pilbara Supergp) - previously assigned to Corboy Fm (now part of Soanesville Gp which overlies this Group). Thickness: up to 1000m. Geol.Prov: Gorge Creek Basin, Pilbara Craton/east Pilbara Terrane. Quartz-rich sandstone.||||||07-FEB-11
70125|Farrel Quartzite|63538|4|Described|p6 Fig. 3|Archean|Archean|Of Gorge Creek Group. Overlain by Cleaverville Formation. Geological Province: Pilbara Craton. Sedimentary rocks.||||||19-APR-13
70125|Farrel Quartzite|64621|5|Briefly described|Map legend|Archean|Archean|Of Croydon Group (De Grey Supergroup). Quartz sandstone and quartzite; locally fuschitic; minor conglomerate and chert; metamorphosed. Brown weathering conglomerate and pebbly sandstone + abundant black chert clasts, weakly metmorphosed.||||||07-NOV-08
70125|Farrel Quartzite|65727|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Gorge Creek Basin, Pilbara Craton.||Of Gorge Creek Group.||Is overlain by Cleaverville Formation.|Quartz sandstone and quartzite; locally fuchsitic; minor agglomerate and chert; metamorphosed.|
70125|Farrel Quartzite|65827|3|Fully described|p6 Tb.1, p16, p28-29, p33||Mesoarchean|Of Gorge Creek Group. Underlies Cleaverville Formation, Mount Roe Basalt (unconformably); unconformably overlies Budjan Creek Formation, Charteris Basalt, Wyman Formation, Euro Basalt. Quartzite intercalated with metachert and conglomerate. At least 1.5 km thick.||||||
70125|Farrel Quartzite|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Unit in Gorge Creek Group. Quartz sandstone and quartzite; locally fuchsitic; minor conglomerate and chert; metamorphosed.||||||
70125|Farrel Quartzite|66109|6|Mentioned|p191, 195-196, 199-201|Archean|Archean|Optical photomicrographs, Raman kerogen images, and confocal laser scanning micrographs of bona fide microfossils.|3050 Ma.|||||
70125|Farrel Quartzite|66122|4|Described|p73-78, 84, 86|Archean|Archean|Mount Goldsworthy greenstone belt, NE Pilbara Craton. Contains a morphologically diverse assemblage of biological structures: threads, films, spheroids and lens-spindles. Simplified stratigraphic column. Chemical analyses of chert samples for REE and Y tabulated and discussed.|c.3.0 Ga.|Gorge Creek Group.||Overlies Warrawoona Group. Is overlain conformably by Cleaverville Formation.|Greenschist-facies metamorphosed, pervasively silicified, fine- to very coarse-grained sandstone including quartzite with minor conglomerate, mafic-ultramafic volcaniclastic layers, evaporite beds and microfossil-bearing black chert layers.|
70125|Farrel Quartzite|66217|4|Described|p5, p30, pp39-41.|Mesoarchean|Mesoarchean|East Pilbara Terrane, Pilbara Craton. Spelt Farrell on p5. Originally assigned to the Corboy Formation of the Gorge Creek Group (Hickman 1983); re-assigned by Van Kranendonk et al. (2006a). Forms main part of the Gorge Range. Deposition was accompanied by normal faulting, indicating extension; thickness to 1000 m. Age from youngest detrital zircon (Nelson 1997).|Max. deposition age of 3058 Ma.|Basal unit in Gorge Creek Group.||Unconformably overlies Wyman Formation. Is overlain conformably by Cleaverville Formation.|Discontinuous, basal polymictic pebble to boulder conglomerate; overlying main unit of white quartzite and quartz-rich sandstone; local unit of interbedded sandstone and siltstone.|
70125|Farrel Quartzite|67197|5|Briefly described|p9, p14, p19, p22, p29, p33-34, p36|||Shown on the legend, but not the map, on p9.||Gorge Creek Group.||||
70125|Farrel Quartzite|67201|4|Described|p7 Fig.4, p12 Tb.1, p20|||In northwestern Pilbara Craton, East Pilbara Terrane, De Grey Superbasin, Gorge Creek Basin. Thickness: varies above basement from few metres to over 1000 m. See Sixty-six Hills Member"". In east Pilbara, U-Pb dating of detrital zircons indicate detritus derived only from the East Pilbara Terrane.||Basal unit in Gorge Creek Group in east Pilbara||Is overlain by Cleaverville Formation.|Predominantly fluviatile polymictic conglomerate and sandstone, with local siltstone, shale, and chert.|
70125|Farrel Quartzite|67668|5|Briefly described|p. 155, p156, 159; Tb.1. Fig. 4. ||Mesoarchean|East Pilbara Terrane, Pilbara Craton. Possible evidence of early life is reviewed. |ca. 3000 Ma.|Gorge Creek Group|||Dominantly clastic sediments with thin inter-beds of black chert and black and white banded chert.|
70125|Farrel Quartzite|68281|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Gorge Creek Basin, De Grey Superbasin, Pilbara Craton.||Of the Gorge Creek Group.|||Quartz-sandstone and quartzite; locally fuchsitic; minor conglomerate and chert; metamorphosed; also polymictic conglomerate, weakly metamorphosed.|23-SEP-13
70125|Farrel Quartzite|68283|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Gorge Creek Basin. Age inferred from age of parent unit.|c.3020 Ma|Of the Gorge Creek Group.|||Quartz sandstone; local basal polymictic conglomerate and siltstone; silicified; metamorphosed.|07-JAN-15
70125|Farrel Quartzite|68284|5|Briefly described|p7|Paleoarchean|Paleoarchean|Kelly greenstone belt, East Pilbara Terrane.|c.3050 Ma.|||Overlies Budjan Creek Formation. Is overlain by Cleaverville Formation.||
70125|Farrel Quartzite|69012|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Gorge Creek Basin.||Of the Gorge Creek Group.|||Pebble conglomerate; metamorphosed.|29-APR-14
70125|Farrel Quartzite|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Gorge Creek Basin. Age constrained by the De Grey Supergroup.||Of the Gorge Creek Group.|||Quartz sandstone and quartzite; locally fuchsitic; minor conglomerate and chert; metamorphosed.|30-APR-14
70125|Farrel Quartzite|69015|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Gorge Creek Basin, De Grey Superbasin.||Of the Gorge Creek Group.|||Sandstone and minor interbedded conglomerate; local siltstone and shale; metamorphosed.|02-MAY-14
70125|Farrel Quartzite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Gorge Creek Group|||Quartz sandstone, lithic arenite, quartz arenite, wacke and quartzite; locally fuchsitic. Carbonate rock; metamorphosed. Siliciclastic sedimentary rocks; metamorphosed. Pebble conglomerate, polymictic conglomerate,pebbly sandstone and shale.|
70125|Farrel Quartzite|69301|4|Described|p5 Fig.3, p9 Tb.1, p14-15, p20 Tb.2, p22|||Pilbara Craton. East Pilbara Terrane. Gorge Creek Basin. Thickness: few metres to >1000 m.|3.05-3.02 Ga|Basal unit of Gorge Creek Group.||Is overlain by Cleaverville Formation.|Mainly composed of fluviatile polymictic conglomerate and sandstone, with local siltstone, shale, and chert; metamorphosed. Exceptionally well preserved microstructures including threads, films, hollow spheres, and spindles.|
70125|Farrel Quartzite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton. Of Gorge Creek Basin, De Grey Superbasin. Events: North Pilbara Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|3066-3022 Ma (inferred)|Unit of Gorge Creek Group.|||Variably silicified and metamorphosed sedimentary rocks; sandstone and quartz sandstone, lithic and quartz arenite, siltstone, shale; conglomerate; pebbly, polymictic.|
70125|Farrel Quartzite|70022|6|Mentioned|p115|||East Pilbara Terrane.||Gorge Creek Group.||||
70125|Farrel Quartzite|70775|5|Briefly described|p12, p46, p48, p57|||Gorge Creek Basin.||Gorge Creek Group||Unconformably overlies the Woodbrook Formation. Overlain by the Cleaverville Formation.|Metamorphosed sandstone and conglomerate.|
70125|Farrel Quartzite|71136|6|Mentioned|p265, 268|||Pilbara Craton. Debate as to whether this unit represents a paleosol (Retallack et al., 2016) or an aqueous deposit (this article).|c.3.0 Ga.|||Is overlain by Cleaverville Formation.|Fossil-bearing carbonaceous black chert.|
70125|Farrel Quartzite|71137|5|Briefly described|p1-9, 11-17|Archean|Archean|Mount Grant area, Pilbara Craton. Contains microfossils. MDA of 3016 +/- 13 Ma (SHRIMP: Nelson, 1998) from upper layer. Fluvial-coastal salina; contains silicified crystals of nahcolite and barite. Folded and faulted into near-vertical dips and isoclinal folds. Lower greenschist facies metamorphosed. Thickness varies from 80m to 1000m. Photomicrographs. Authors argue for a paleosol environment. Morphotypes tabulated.|3.0 Ga.|Gorge Creek Group.||Unconformably overlies Kelly and Warrawoona Groups. Is overlain conformably by Cleaverville Formation.|Basalt trough cross-bedded sandstone and conglomerates; quartz-lithic sandstone, lesser claystone, tuff beds, black chert clasts with microfossils.|
70125|Farrel Quartzite|71138|6|Mentioned|p270|Archean|Archean|The authors recapitulate the evidence for paleosols in this microfossil-bearing unit.||||||
70125|Farrel Quartzite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Gorge Creek Basin.||Gorge Creek Group|||Quartz sandstone and quartzite; locally fuchsitic; minor conglomerate and chert; metamorphosed.|
70125|Farrel Quartzite|72251|5|Briefly described|p51,54,64|Mesoarchean|Mesoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Contains 3.71-3.5 Ga detrital zircon grains (Sheppard et al., 2017), could indicate existence of even older crust within the EPT.||Unit of Gorge Creek Group.||Lowermsot unit of Gorge Creek Group. Overlain by, and equivalent to Cleaverville Formation, or unconformably by Coonieena Basalt. Underlain by Pyramide Hill Formation or Honeyeater Basalt.||
70125|Farrel Quartzite|72487|6|Mentioned|p10|Archean|Archean||3.0 Ga.|||||
70125|Farrel Quartzite|72668|5|Briefly described|p4, p14|||East Pilbara Terrane. Up to 1000 m thick. Detrital zircon populations are of old populations characteristic of the East Pilbara.||Gorge Creek Group||Overlain by the Cleaverville Formation.|Basal conglomerate and quartz-rich sandstone.|13-JAN-22
70125|Farrel Quartzite|73598|6|Mentioned|p1212|Mesoarchean|Mesoarchean|East Pilbara Terrane.||Gorge Creek Group.||Unconformably overlies Pyramid Hill Formation. Is overlain by Cleaverville Formation.||
31386|Faure Formation|1943|2|Defined|p388, p373, Fig. 3,4,10 on p375-6 & p383|||New unit. Equivalent to upper part of Dirk Hartog Limestone Unit A and lower Kopke Sandstone of Hocking et al. (1987). Type section in Yaringa-1 (820-947m). Max. thickness: 138m in Tamala-1. Age: possible Devonian age (G.C. Young, pers. comm., 1994).||||Unconformably overlies Hamelin Formation (Dirk Hartog Group). Oversteps Hamelin Formation to lie unconformably on Ajana Formation in Wandagee-1. Upper boundary not well controlled.|Reddish silty sandstones, siltstones and claystones. Angular carbonate clasts (probably reworked from top of underlying Ajana Formation).|
31386|Faure Formation|6943|5|Briefly described|p599, pp601-605.|Early Devonian|Early Devonian|Previously, uppermost part of Dirk Hartog Formation.||||Unconformably overlies Coburn Formation. Is overlain by Kopke Sandstone.|Shale, dolomite, minor sandstone.|
31386|Faure Formation|12471|6|Mentioned|p475 Fig.2. |Early Devonian|Early Devonian|||||||
31386|Faure Formation|12729|4|Described|p.10-11, 28, 32; Figs. 3-4, 6-10, 22-4|Early Devonian|Early Devonian|Previously of 'Dirk Hartog Formation'. Modified after Gorter et al. (1994). Type section: 855-947 m in Yaringa 1. 72-149 m thick. Basal contact: sharp change in colour and S isotopes. Early Devonian deduced from stratigraphic position. Palynomorphs suggest pre-Givetian.  ||||Unconformably overlies the Dirk Hartog Group, conformably underlies the Kopke Sandstone.|Consists of mudstone, dolomite, and fine-grained sandstone. Deposited in a low-energy, saline to hypersaline, shallow-water environment in an arid climate.|
31386|Faure Formation|12731|5|Briefly described|p590 Fig.2.|Early Devonian|Early Devonian|Dolomite might be a potential hydrocarbon reservoir.||||Is overlain by Kopke Sandstone.|Mixed siliciclastics and dolomite.|
31386|Faure Formation|12733|5|Briefly described|p554 Fig.2.|Early Devonian|Early Devonian|Lochkovian.||||Is overlain by Kopke Sandstone.|Carbonate and siliciclastic deposits.|
31386|Faure Formation|13996|6|Mentioned|p148|Middle Devonian|Middle Devonian|Contains microvertebrate remains (?from a reworked Silurian limestone pebble); species listed.||||||
31386|Faure Formation|14227|5|Briefly described|Enclos. 2|||Presented as Faure only - Formation inferred.||||||07-FEB-11
31386|Faure Formation|14228|5|Briefly described|p5 fig2, p6 fig3, p7, p18|Lochkovian|Lochkovian|Gascoyne Platform. Thickness 72 - 149m. May act as a seal.||||Overlain conformably by Kopke Sandstone.|Mudstone, dolomite, gypsum.|
31386|Faure Formation|23572|4|Described|p8 Fig. 6, p10|Lochkovian|Lochkovian|Geological Province: Carnarvon Basin. Underlying Unit: Dirk Hartog Group (disconformable). Overlying Unit: Kopke Sandstone (conformable). Max. thickness: 149m.||||||
31386|Faure Formation|23726|5|Briefly described|p13|||Overlying unit Kopke Sandstone. Underlying unit Dirk Hartog Sandstone.||||||
31386|Faure Formation|23935|4|Described|p11 Fig.7|Lochkovian|Lochkovian|Unconformably overlies Coburn Formation. Conformably overlain by Kopke Sandstone. Geological Province: Southern Carnarvon Basin.||||||
31386|Faure Formation|24390|5|Briefly described|p19 Fig. 10|Devonian||Geological Province: Southern Carnarvon Basin.||||||
31386|Faure Formation|43566|6|Mentioned|Fig.2,p415|||||||||
31386|Faure Formation|49942|4|Described|p4 Fig.3, p9|Early Devonian|Early Devonian|Conformably overlain by Kopke Sandstone. Disconformably overlies Dirk Hartog Group. Max. thickness: 150 m. Mudstone, dolomite and fine grained sandstone. Depositied in saline-hypersaline low energy arid environment. Geological Province: Gascoyne Platform.||||||
31386|Faure Formation|50084|4|Described|p77|Middle Devonian|Early Devonian|Grey to red mudstone and dolostone. Overlies Coburn Formation following a hiatus. Conformably overlain by Kopke Sandstone. Thickness: 66 m. Geological Province: Southern Carnarvon Basin.||||||07-FEB-11
31386|Faure Formation|50085|5|Briefly described|p19 Fig. 10|Devonian|Devonian|Geological Province: Southern Carnarvon Basin.||||||
31386|Faure Formation|60384|5|Briefly described|p244, p243 Fig 2a|Early Devonian|Early Devonian|Southern Carnarvon Basin.||||Conformably overlain by Kopke Sandstone|Mudstone, dolomite and fine-grained sandstone|
31386|Faure Formation|60725|5|Briefly described|p29; p35-36 Figs.5,6; p36. |Early Devonian|Early Devonian|Has potential as a seal for reservoirs in Dirk Hartog Group.||||Is overlain by Kopke Sandstone.|Carbonate and siliciclastics.|10-MAY-17
31386|Faure Formation|61023|5|Briefly described|p34 Fig. 14|Devonian|Devonian|Geological Province: Southern Carnarvon Basin.||||||11-APR-08
31386|Faure Formation|64635|6|Mentioned|p6 ||||||||Shallow-marine mixed siliciclastic rocks and dolomite.|
31386|Faure Formation|64972|6|Mentioned|p617 Fig. 5|Early Devonian|Early Devonian|||||||25-MAY-21
31386|Faure Formation|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes bioturbated grey/red/brown claystone.|
31386|Faure Formation|67200|5|Briefly described|p7 fig 5|Devonian|Devonian|Thermal conductivity of 1.62 W/mK. See also p18 table 1, p46, p51, p55, app 2 tbl 1 p4. ||||Overlies Dirk Hartog Sandstone, overlain by Kopke Sandstone|Parallel bedded limestone, bioturbated claystone.|
31386|Faure Formation|69029|6|Mentioned|p326,328|Lochkovian|Lochkovian|Of onshore Carnarvon Basin.||||Overlain by Kopke Sandstone. Underlain by Dirk Hartog Group.||
31386|Faure Formation|69182|5|Briefly described|Ch3 p8, Ch3 p10-p11|Early Devonian|Early Devonian|Carnarvon Basin. Deposited in a low-energy saline to hypersaline, shallow water environment under arid conditions. See also  Ch3 p23, Ch3 p35, Ch3 p37, Ch3 p67-p68, Ch3 p73.  ||||Conformably overlain by the Kopke Sandstone.|Mudstone, dolomite and gypsum.|
31386|Faure Formation|69297|5|Briefly described|p249|Lochkovian|Lochkovian|Gascoyne Sub-basin of the Southern Carnarvon Basin. ||||Overlies the Coburn Formation. Overlain by the Kopke Sandstone.|Limestones.|
31386|Faure Formation|69558|6|Mentioned|p106|Early Devonian|Early Devonian|Of Iasky and Mory (1999).||||||25-MAY-21
31386|Faure Formation|71146|5|Briefly described|p6|Lochkovian|Pridoli|Southern Carnarvon Basin.||||Disconformably overlies the Coburn Formation. Overlain by the Kopke Sandstone.|Carbonate and mudstone.|
24978|Ferro Gully Shale|33687|6|Mentioned|Fig.1|||||||||
79008|Fields Find Igneous Complex|69583|6|Mentioned|p49|Mesoarchean|Mesoarchean|Murchison Domain.||||||
79008|Fields Find Igneous Complex|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean|||Meeline Suite||||
79008|Fields Find Igneous Complex|69586|5|Briefly described|p22|Mesoarchean|Mesoarchean|Murchison Domain.||Meeline Suite.||||
79008|Fields Find Igneous Complex|71272|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Boodanoo Suite.||||
79008|Fields Find Igneous Complex|71809|5|Briefly described|map legend|Archean|Archean|Yilgarn Craton||Of Boodanoo Suite.|||Dolerite, local gabbro, metamorphosed; gabbro, local gabbronorite; pyroxenite, locally with peridotite, gabbro; hornblende-bearing pyroxene peridotite, typically serpentinised, metamorphosed; interlayered pyroxenite and peridotite.|
80938|Fifima Sandstone|72049|5|Briefly described|p256|||Zircon geochronology shows a subpopulation dated at roughly 2690 Ma and 1 older grain at roughly 2816 Ma (U-Pb zircin SHRIMP dating).|c. 2704 Ma|||||18-MAR-19
26551|Fifty Mile Tank Gneiss|24223|5|Briefly described|Map legend|Archean|Archean|Quartzo-feldspathic gneisses.||||||07-NOV-08
26551|Fifty Mile Tank Gneiss|41771|4|Described|p32|||||||||
26551|Fifty Mile Tank Gneiss|42221|5|Briefly described|p10|||||||||
26551|Fifty Mile Tank Gneiss|42724|5|Briefly described|map legend|Archean||||||||07-NOV-08
26551|Fifty Mile Tank Gneiss|42817|4|Described|p20|||||||||
26551|Fifty Mile Tank Gneiss|60076|5|Briefly described|p24, p46 App. 1|Archean|Archean|[Anfi] Quartzo-feldspathic, porphyropyroclastic; minor monzogranite; schistose mafic to ultramafic enclaves common. Banded gneiss with strong foliation. Parts with deformed pegmatite veins. Age: 2664+/-5Ma (U-Pb SHRIMP, Nelson 1995). Of the Pioneer Dome||||||07-NOV-08
26551|Fifty Mile Tank Gneiss|65264|5|Briefly described|p25, p47 Appdx. 1|Archean|Archean|A major feature of the Pioneer Dome in southern part of the Kalgoorlie terrane. Also written informally as Fifty Mile Tank gneiss (p25). Quartzo-feldspathic gneiss; porphyroclastic; minor monzogranite; schistose mafic to ultramafic enclaves common.||||||05-AUG-15
26551|Fifty Mile Tank Gneiss|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||Includes unnamed pegmatitic subunit.||Quartzofeldspathic gneiss, porphyroclastic; minor monzogranite; schistose mafic to ultramafic enclaves common; quartzofeldspathic gneiss with numerous deformed pegmatite veins.|05-AUG-15
26551|Fifty Mile Tank Gneiss|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Quartzofeldspathic gneiss, porphyroclastic; minor monzogranite; schistose mafic to ultramafic enclaves common.|
26551|Fifty Mile Tank Gneiss|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||felsic gneiss, monzogranite, greenstone, pegmatite|
26551|Fifty Mile Tank Gneiss|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. See 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|||||Quartzofeldspathic gneiss, porphyroclastic; minor monzogranite; schistose mafic to ultramafic enclaves common; numerous deformed pegmatite veins.|
39513|Fig Tree Gneiss|63417|5|Briefly described|Map legend|Archean|Archean|Of the Tambina Supersuite.  Geological Province: Pilbara Craton. Banded tonalite, granodiorite, and local trondhjemite, monzogranite and syenogranite, gneiss and migmatite.||||||07-NOV-08
39513|Fig Tree Gneiss|63441|5|Briefly described|p7 Tb. 2|Archean|Archean|Of the Tambina Supersuite. Age: 3448+/-8 to 3429+/-13Ma. Geological province: Pilbara Craton.||||||07-FEB-11
39513|Fig Tree Gneiss|64621|5|Briefly described|Map legend|Archean|Archean|Of the Tambina Supersuite. Banded tonalite; inequigranular; medium- to coarse-grained; varies from homogeneous, to schlieric-textured, to locally gneissic; metamorphosed.||||||07-NOV-08
39513|Fig Tree Gneiss|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.|c.3430 Ma (Nelson 2002).|Of Mount Edgar Granitoid Complex.|||Mixed banded, migmatitic, and granitic gneisses; tonalite, granodiorite, and minor monzogranite and syenogranite compositions; includes strongly foliated and gneissic tonalite, granodiorite, and monzogranite intrusions.|
39513|Fig Tree Gneiss|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c.3440 Ma.|Of Tambina Supersuite.|||Banded tonalite, granodiorite, and local trondhjemite, monzogranite and syenogranite gneiss and migmatite; similar lithologies with numerous mafic xenoliths are mapped separately.|
39513|Fig Tree Gneiss|65827|2|Defined|p6,12,13 Tbs.2,3,4; p15, p20, p27, p59|Paleoarchean|Paleoarchean|New name; after Fig Tree Well. Exposed in several areas. 3435+/-3 Ma (SHRIMP U-Pb zircon; Bodorkos et al. 2006) to 3430+/-4 Ma (Nelson 2002). 3448-3426 Ma protolith emplacement; metamorphism and partial melting c.3325-3315 Ma. Intruded by Kennell, Chessman and Joorina Granodiorites, Moolyella Monzogranite, Davitt Syenogranite. Protoliths intruded, and are now in sheared contact with, Underwood Gneiss protoliths. Intruded by Warrawoona Group, Brockman Creek Kimberlite; underlies Panorama Formation. Mis-spelt as Fig Tree gneiss on p58. Hosts gold-bearing quartz veins.||Of Tambina Supersuite.|||Synvolcanic TTG bodies: banded gneiss, migmatite, granitic gneiss; gneissic intrusions with compositions ranging from tonalite and granodiorite to monzogranite and syenogranite.|21-MAY-14
39513|Fig Tree Gneiss|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Tambina Supersuite. Age shown as 3448-3416 Ma. Banded metatonalite, metagranodiorite, and local metatrondhjhemite, monzogranite and syenogranite gneiss, and migmatite.||||||
39513|Fig Tree Gneiss|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Age derived from sample of monzogranite gneiss (178079.1.pdf) and is the age of cryztallization of monzogranite protolith.|3416 +/-8 Ma (SHRIMP)|Tambina Supersuite||Intruded by Johansen Monzogranite|Banded metatonalite, metagranodiorite, metamonzogranite, metasyenogranite and local metatrondhjemite, monzogranite and syenogranite gneiss, and migmatite. Interlayered granitic gneiss and mafic amphibolite.|
39513|Fig Tree Gneiss|69566|6|Mentioned|p236|||Mount Edgar Granitoid Complex, East Pilbara Granite-Greenstone Terrane.||Tambina Supersuite.||||
39513|Fig Tree Gneiss|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA 178079 (leucocratic monzogranite gneiss) yielded an interpreted igneous crystallisation age of 3416+\-8 Ma for the monzogranite (weighted mean 207Pb/206Pb). Sample GSWA 178100 (leucotonalite) yielded an interpreted igneous crystallisation age of 3435+\-3 Ma for the monzogranite (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3448-3416 Ma (isotopic, inferred)|Unit of Tambina Supersuite.||Intruded by Johansen Monzogranite and Kennell Granodiorite. In fault contact with Homeward Bound Granite.|Banded metatonalite, metagranodiorite, metamonzogranite, and local metatrondhjemite, monzogranite and syenogranite gneiss, and migmatite|
39513|Fig Tree Gneiss|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||felsic gneiss, migmatite|
39513|Fig Tree Gneiss|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||Max age 3448+/-8 Ma, min 3416+/-8 Ma|Tambina Supersuite|||Banded metatonalite and metagranodiorite gneiss; local metatrondhjemite, metamonzogranite and metasyenogranite gneiss, and migmatite.|
73451|Fingoon Package|65454|4|Described|p4, p7 Fig.3, p30 Fig.A1b|Statherian|Statherian|Talbot Terrane and may have equivalents in Connaughton Terrane. Of Rudall Complex. Metasedimentary succession comprising Larry Formation, Fingoon Quartzite, Butler Creek Formation, Poynton Formation and Yandagooge Formation. Age uncertain but experienced Yapungku Orogeny ~1800-1760 Ma or ~1680 Ma, and an earlier event?|~1800-1760 Ma|||||17-AUG-18
31761|Finlayson Member|12099|5|Briefly described|p678 Fig.4|Paleoproterozoic|Orosirian|Equivalent to Finlayson Sandstone of Gee (1987) and Finlayson Sandstone Member of Gee and Grey (1993)?||Unit in Juderina Formation.||||04-MAR-13
31761|Finlayson Member|22694|5|Briefly described|p7|||||||||
31761|Finlayson Member|22940|4|Described|Table 2 p12|||of Juderina Formation, Yerrida Group.||||||
31761|Finlayson Member|23133|5|Briefly described|p293 Fig.1|||of Yerrida Basin.||||||
31761|Finlayson Member|23413|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Juderina Formation, Yerrida Basin||||||
31761|Finlayson Member|23581|5|Briefly described|Map legend||Paleoproterozoic|Of the Juderina Formation in the Windplain Subgroup in the Yerrida Group in the Yerrida Basin||||||07-NOV-08
31761|Finlayson Member|23586|4|Described|p15|Paleoproterozoic|Paleoproterozoic|Of Juderina Formation. Overlying unit Bubble Well Member. Geological Province: Yerrida Basin.||||||07-NOV-08
31761|Finlayson Member|23589|5|Briefly described|p15|||Of Juderina Formation.||||||
31761|Finlayson Member|23593|4|Described|p7|||Of Juderina Formation. Overlying unit Bubble Well Member. Geological Province: Yerrida Basin.||||||
31761|Finlayson Member|23600|5|Briefly described|p8|||Of Juderina Formation. Overlying unit Bubble Well Member. Geological Province: Yerrida Basin.||||||
31761|Finlayson Member|23611|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|See also page 33 Appendix 1. Of Windplain Subgroup. Geological Province: Yerrida Basin.||||||07-NOV-08
31761|Finlayson Member|23744|4|Described|p10|Paleoproterozoic|Paleoproterozoic|Formerly Finlayson Sandstone Member. See also page 10 table 1. Of Juderina Formation. Geological Province: Yerrida Basin. Max. thickness 50 m.||||||07-NOV-08
31761|Finlayson Member|23747|5|Briefly described|p4 table 1|Paleoproterozoic|Paleoproterozoic|Of Juderina Formation. Geological Province: Yerrida Basin.||||||07-NOV-08
31761|Finlayson Member|23749|4|Described|p6|Proterozoic|Proterozoic|Formerly Finlayson Sandstone Member.  Of Juderina Formation. Geological Province: Yerrida Basin.||||||
31761|Finlayson Member|23759|4|Described|p15|Paleoproterozoic|Paleoproterozoic|Of Juderina Formation. Overlying unit Bubble Well Member. Geological Province: Yerrida Basin.||||||07-NOV-08
31761|Finlayson Member|24021|5|Briefly described|p12|Paleoproterozoic|Paleoproterozoic|Parent: Juderina Formation.   Geological Province: Yerrida Basin||||||07-NOV-08
31761|Finlayson Member|24022|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Juderina Formation. Geological Province: Yerrida Basin.||||||07-NOV-08
31761|Finlayson Member|24028|5|Briefly described|p289|Paleoproterozoic|Paleoproterozoic|Of Juderina Formation.  Geological Province: Yerrina Basin.||||||07-NOV-08
31761|Finlayson Member|43831|5|Briefly described|Map Legend||Paleoproterozoic|of Juderina Formation.||||||07-NOV-08
31761|Finlayson Member|43836|5|Briefly described|Map Legend||Proterozoic|of Juderina Formation.||||||
31761|Finlayson Member|43837|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Juderina Formation (Windplain Subgroup, Yerrida Group).  Quartz arenite, commonly ripple-marked.||||||18-MAY-04
31761|Finlayson Member|43843|5|Briefly described|Map Legend||Proterozoic|||||||
31761|Finlayson Member|44204|5|Briefly described|Map Legend||Proterozoic|Of Juderina Formation.||||||
31761|Finlayson Member|49893|4|Described|p9|Proterozoic|Proterozoic|Of the Juderina Formation (Yerrida Group). Geological Province: Yerrida Basin. Max. thickness: ~100m. Overlian by and interfingers with the Bubble Well Member. See also p3 Table 1.||||||
31761|Finlayson Member|49912|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Juderina Formation (Yerrida Group).  Quartz arenite and subordinate siltstone; planar-bedded or cross-stratified; commonly ripple-marked.  Geological Province: Yerrida Basin.||||||
31761|Finlayson Member|50222|5|Briefly described|p320 Fig. 3, p321|Paleoproterozoic|Paleoproterozoic|Of the Juderina Formation (Windplain Group).  Contains detrital zircons of Archaean age: 2.7Ga (Hallovic, unpub/in progress).||||||07-NOV-08
31761|Finlayson Member|62289|4|Described|plate 1, p6-7, p9-p10, p29|Palaeoproterozoic|Palaeoproterozoic|Occhipinti et al. (1997). Base of the Juderina Formation, Windplain Subgroup, Yerrida Group. Consists of basal quartz arenite (<100m, individual beds few cm to 1 m thick); local pseudomorphs after halite; minor shale, siltstone; minor ferruginous quartz arenite (red beds) of this unit are intercalated with evaporites of the Bubble Well Member. Unconformably overlain by Yelma Formation.||||||
31761|Finlayson Member|62353|5|Briefly described|map legend|Proterozoic|Proterozoic|Geol. Prov: Yerrida Basin.||Of Juderina Formation.||Disconformable over Archaean basement.|Quartz arenite; planar bedded on cross-stratified minor pebble conglomerate and intercalated siltsone.|14-APR-11
31761|Finlayson Member|64580|4|Described|map legend||Paleoproterozoic|Of Juderina Formation. Quartz arenite; planar bedded or cross-bedded minor pebble conglomerate and intercalated siltstone.||||||15-DEC-08
31761|Finlayson Member|65264|5|Briefly described|p27|||Of Juderina Formation (Windplain Subgroup). Geological province: Yerrida Basin. Sedimentary sequence of mature siliciclastic arenite, cross-stratified conglomerates and intercalated siltstone deposits.||||||07-FEB-11
31761|Finlayson Member|65411|5|Briefly described|p88.|Paleoproterozoic|Paleoproterozoic|||Basal unit in Yerrida Group.|||Quartz arenite.|
31761|Finlayson Member|65419|1|Redefined|p8, pp10-15.|Paleoproterozoic|Paleoproterozoic|Gee and Grey (1993) incorporated the Finlayson Sandstone as a Member into the Juderina Formation. Renamed the Finlayson Member (Occhipinti et al. 1997) because of its heterolithic nature. From a few tens of metres to a maximum of a few hundred metres thick. Type section described.  Reference section at Mount Alice.||Basal unit in Juderina Formation.||Is intruded or overlain by Killara Formation. Is conformably overlain by Bubble Well Member. Is locally unconformably overlain by Earaheedy Group.|Fine-medium grained well-bedded and cross-bedded quartz arenite; hematitic quartz arenite; shale and siltstone beds; rounded siltstone concretions; minor carbonate.|13-NOV-13
31761|Finlayson Member|65472|5|Briefly described|p3 Fig.2|||Yerrida Basin. Age: from Fig.2, after Pirajno et al. 2004.|2.7 Ma detrital zircon U-Pb SHRIMP youngest age|||||
31761|Finlayson Member|65550|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Juderina Formation, Windplain Group, Yerrida Basin. Quartz arenite; planar or cross bedded; minor pebble conglomerate and intercalated siltstone.||||||
31761|Finlayson Member|65896|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Basal Member of Juderina Formation, Yerrida Group, Yerrida Basin. Quartz arenite and finely bedded siltstone.||||||
31761|Finlayson Member|65913|4|Described|p3 Table 1, p5, p20. |Paleoproterozoic|Paleoproterozoic|Similar to the base of the Yelma Formation in Earaheedy Group; the latter has coarser grain size, thicker bedding, weaker cementation, and abundance of trough cross-bedding.||Basal unit in Juderina Formation.||Is overlain by Juderina Formation.|Mauve to pinkish, fine- to medium-grained, mature quartz arenites; some quartz granule beds, rare quartz-pebble lags; planar and trough cross-beds and ripple marks common; well-jointed with blocky weathering; lesser interlayered mauve siltstone.|
31761|Finlayson Member|66427|5|Briefly described|p51 |||||Of the Juderina Formation.||Is overlain unconformably by Yelma Formation.|Quartz arenite.|
31761|Finlayson Member|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Paleoproterozoic|Paleoproterozoic|Yerrida Basin, Capricorn Orogen||Juderina Formation|||Quartz arenite; planar or cross bedded; minor pebble conglomerate and intercalated siltstone|
31761|Finlayson Member|69003|5|Briefly described|p12|||Yerrida Basin.||Juderina Formation.||Is overlain conformably by Maraloou Formation.||
31761|Finlayson Member|69152|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin [??]||Juderina Formation|||Quartz arenite; planar or cross bedded; minor pebble conglomerate and intercalated siltstone.|24-SEP-15
31761|Finlayson Member|69166|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|||Juderina Formation|||Quartz arenite; planar bedded or cross-bedded minor pebble conglomerate and intercalated siltstone.|
31761|Finlayson Member|69596|6|Mentioned|p10|||Yerrida Basin.||Juderina Formation.||||
31761|Finlayson Member|70153|5|Briefly described|100k_geologyp10_lut.csv|Paleoproterozoic|Paleoproterozoic||c.1298 Ma (inferred).|Juderina Formation|||Quartz arenite; planar or cross bedded; minor pebble conglomerate and intercalated siltstone.|
31761|Finlayson Member|70796|5|Briefly described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|West Australian Craton, Yerrida Basin, Capricorn Orogen. See also 100k_interpgeop_lut.csv, Glengarry100_2645_stratig.pdf.|ca. 2170 to 1600 Ma (inferred)|Juderina Formation|||Quartz arenite; rippled, planar or cross bedded; minor pebble conglomerate and intercalated siltstone|
31761|Finlayson Member|70804|5|Briefly described|p2, p19, plate 1|||Replaces the obsolete Finlayson Sandstone.||Juderina Formation|||Quartz arenite.|27-FEB-23
31761|Finlayson Member|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone, sedimentary breccia|
31761|Finlayson Member|71269|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen, West Australian Craton. Of Yerrida Basin. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 1m_geologyp12_lut.csv, glengarry_100k_geologyp_lut.csv.|2170-1600 Ma (inferred)|Unit of Juderina Formation.|||Off-white silica-cemented rippled mature thinly to thickly bedded quartz sandstone and quartz siltstone with local brown diagenetic spots; local chert breccia. Quartz arenite.|
31761|Finlayson Member|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen. Of Earaheedy Basin. See 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.||Unit of Juderina Formation.|||Quartz arenite; planar or cross bedded; minor pebble conglomerate and intercalated siltstone|
31761|Finlayson Member|71484|4|Described|p124-125,127,130,133|Rhyacian|Rhyacian|Geological province: Of Yerrida Basin. Thickness: up to several hundred meters. Transgressive sand, recording the initial marine transgression over the NW Yilgarn Craton at the start of Windplain deposition.||Unit of Juderina Formation.||Basal unit of Juderina Formation. Overlain by Bubble Well Member.|Arkosic sandstone and quartz wacke; minor conglomerate, quartz siltstone, laminated quartz sandstone.|30-AUG-19
75076|Fishburn Formation|67370|2|Defined|pp313-314, pp316-318,  p332, p334.|Early Triassic|Early Triassic|Defined. Named after Fishburn-1; type section is between 1,904.5 - 2,084 m. Contains the K. saeptatus Oppel Zone (P. samoilovichii Oppel Zone). Nearshore, mostly transgressive,  depositional environment. Widespread unit in Bonaparte Basin. The top of this unit is an erosional surface below the Osprey Formation (eastern Bonaparte Basin) and Sahul Group (western Bonaparte, northern Browse Basins).||Topmost unit in Mount Goodwin Subgroup.||Overlies Ascalon Formation. Is overlain unconformably by Cape Londonderry Formation (in the east) and Sahul Group (in the west).|Grey and green claystones with minor siltstone and sandstone.|
75076|Fishburn Formation|69452|3|Fully described|p36:8, 15, 20-21|Anisian|Olenekian|Gorter et al. (2009). Equivalent to the Upper Mount Goodwin Formation of Gorter (1998). Petrel Sub-basin, Bonaparte Basin. Widespread offfshore, but is truncated by erosion towards the southern margin and is not recognised onshore. 179.5m thick in the type section in drillhole Fishburn-1.||Mount Goodwin Subgroup.||Conformably and transitionally overlies Ascalon Formation.|Claystone with minor siltstone and sandstone.|12-JUL-16
75076|Fishburn Formation|69454|5|Briefly described|p38:4|Olenekian|Olenekian|Petrel Sub-basin, Bonaparte Basin.||Mount Goodwin Subgroup.||||12-JUL-16
75076|Fishburn Formation|69653|6|Mentioned|p10|Early Triassic|Early Triassic|Petrel Sub-basin.||Mount Goodwin Sub-group.||Overlies Ascalon Formation. Is overlain by Lower Cape Londonderry Formation (Troughton Group).||
75076|Fishburn Formation|69673|6|Mentioned|p153 fig 125|||||Mount Goodwin Subgroup||Overlain by Cape Londonderry Formation, overlies Ascalon Formation||
75076|Fishburn Formation|70061|5|Briefly described|Petrel Sub-basin Figs.2 & 3|Olenekian|Olenekian|See also Regional geology: Figs.6-7. Vulcan: Fig.2.||Mount Goodwin Subgroup.||Overlies Ascalon Formation.||12-JUL-16
38799|Fisher Basalt|23926|6|Mentioned|p33 Fig. 15|||Geological Province: Yilgarn Craton.||||||
38799|Fisher Basalt|23931|6|Mentioned|p200 Fig.2|||Geological Province: Yilgarn Craton.||||||
35858|Fitzgerald Member|23331|3|Fully described|1095|||||||||10-SEP-09
35858|Fitzgerald Member|23488|5|Briefly described|p40|||Of Pallinup Siltstone.  Geological Province: Bremer Basin.||||||
35858|Fitzgerald Member|23533|5|Briefly described|p564|Late Eocene|Late Eocene|See also Fig. 3. Of Pallinup Formation. Geological Province: Bremer Basin.||||||
35858|Fitzgerald Member|24397|4|Described|p243|||Of the Pallinup Formation.  Geological Province: Eucla Basin.||||||
35858|Fitzgerald Member|24557|5|Briefly described|p958, p959 Fig.2|Late Eocene|Late Eocene|Of the Pallinup Formation, uppermost unit. Sponge dominated. Geological Province: Bremer Basin.||||||
35858|Fitzgerald Member|69598|5|Briefly described|p2, p9, p10, p11 Tb.1, p29 Tb.4|Late Eocene|Late Eocene|Eucla Basin. Potential carbon dioxide storage reservoir.||Pallinup Formation||||
26555|Fitzroy Volcanics|23765|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
26555|Fitzroy Volcanics|23766|5|Briefly described|p30|||Consists of a leucite lamproite.   Thickness: 45m.||||||
26555|Fitzroy Volcanics|42710|5|Briefly described|map legend|Miocene||Variation on Fitzroy Lamproite.||||||
26555|Fitzroy Volcanics|42811|4|Described|p45|||||||||
26555|Fitzroy Volcanics|43281|5|Briefly described|Map legend|Tertiary|Tertiary|Canning Basin||||||
26555|Fitzroy Volcanics|64580|4|Described|map legend||Miocene|Lamproite and associated pyroclastic rock.||||||09-DEC-08
26555|Fitzroy Volcanics|65486|6|Mentioned|Plate 1|Miocene|Miocene|Lamproite diatremes in the Fitzroy Trough, Canning Basin.||||||
26555|Fitzroy Volcanics|66127|5|Briefly described|Plates 1, 2, 3, 7, 8.|Miocene|Miocene|Small plugs, <100 m to 1.8 km across; several, known as the Ellendale Vents, are diamondiferous.|||||Lamproite diatremes and associated pyroclastic rocks, largely or entirely covered by Quaternary soils.|
26555|Fitzroy Volcanics|69099|5|Briefly described|500k_geologyp08_lut.csv||Miocene||||||Lamproite and associated pyroclastic rock.|31-JUL-15
26555|Fitzroy Volcanics|69165|4|Described|500k_geologyp08_lut.csv||||||||lamproite and associated pyroclastic rock.|
26555|Fitzroy Volcanics|69634|5|Briefly described|500k_geologyp08_lut.csv||Miocene||||||Lamproite and associated pyroclastic rock|
26555|Fitzroy Volcanics|70126|5|Briefly described|Map legend|Miocene|Miocene||22-18 Ma (Jaques et al., 1984).||||Lamproite and associated pyroclastic rock.|
26555|Fitzroy Volcanics|70154|5|Briefly described|100k_geologyp_lut.csv|Miocene|Miocene|See also 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|18-22 Ma||||Lamproite and associated pyroclastic rock.|
26555|Fitzroy Volcanics|71267|4|Described|GEOL_LUT_CSV files|Miocene|Miocene|Of Fitzroy Trough, Lennard Shelf, Canning Basin. See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyp_lut.csv.|22+\-4 to 18+\-4 Ma (isotopic)||||Leucite lamproite, olivine lamproite, lapilli and chaotic tuffs|
26555|Fitzroy Volcanics|71892|6|Mentioned|p10|Cenozoic|Cenozoic|||||||
26555|Fitzroy Volcanics|72034|5|Briefly described|500k_interpgeop16_lut|Miocene|Miocene|Fitzroy Trough; Lennard Shelf, Canning Basin.|Max age 22+/-4 Ma, min age 18+/-4 Ma.||||Lamproite and associated pyroclastic rock.|
27407|Flacourt Formation|12471|6|Mentioned|p476, p486.|||Has late carbonate cement. A residual oil-leg is evident from hydrocarbon inclusions within early quartz overgrowths. Is what the Nannutarra Formation section in Tunbridgi 7 and 8  was reassigned to by Thompson (1992), but this paper prefers original interpretation (Nannutarra Fm).||||||27-OCT-14
27407|Flacourt Formation|13615|3|Fully described|p4-p5, p12, p18-p19, p35, p38|Valanginian|Tithonian|Ashburton Embayment, Peedamullah Shelf and Onslow Terrace. <60m thick onshore but reaches >600m thick offshore. Spores/Pollen Zone and Dinoflagellate zones provided. Deltaic depositional environment. Porosity of this unit is provided. Rocks previously assigned to the Yarraloola Conglomerate and Birdrong Sandstone in multiple drillholes have been reassigned to the Flacourt Formation. Type section occurs in Barrow 1 drillhole between 914-1370m. Contains sparse microfauna. Deposited in a delta topset or upper forset environments. Overlain by the Birdrong Sandstone. Unconformably overlain by the Mardie Greensand. Equivalent to the Yarraloola Conglomerate. See also p40, p43, p45, p48-p53, p56, p58, p65-p68, p70-p71, p78, p81-p83, p85, p87-p88, p102  App. 3, p118.||of Barrow Group.||Overlies the Dingo Claystone. Unconformably overlies the Mungaroo Formation and Chinty Formation.  Likely time equivalent to Yarraloola Conglomerate + Nannutarra Formation.|Fine-grained to pebble-sized, poorly sorted and partially cemented sandstone.|07-FEB-19
27407|Flacourt Formation|23355|6|Mentioned|13|||||||||
27407|Flacourt Formation|23379|4|Described|p160 Fig.2;p158,159,162,163,167-174|Valanginian|Berriasian|of Barrow Group, Barrow Sub-basin, Carnarvon Basin.||||||
27407|Flacourt Formation|23726|5|Briefly described|p8 Fig 2c|Early Cretaceous|Early Cretaceous|Overlying unit Mardi Greensand Member. Underlying unit Malouet Formation. Geological Province: Carnarvon Basin.||||||
27407|Flacourt Formation|24331|5|Briefly described|p475 Fig.2|Early Cretaceous|Early Cretaceous|Conformably overlies Malouet Formation. Unconformably overlain by Mardie Greensand Member. Marine to fluvial. Geological Province: Barrow Sub-basin.||||||
27407|Flacourt Formation|24390|5|Briefly described|p24 Table 6|||Geological Province: Northern Carnarvon Basin.||||||
27407|Flacourt Formation|37689|6|Mentioned|p24|||||||||
27407|Flacourt Formation|40617|6|Mentioned|p12|||||||||
27407|Flacourt Formation|41271|3|Fully described|p140|||||||||
27407|Flacourt Formation|41438|6|Mentioned|p108|||||||||
27407|Flacourt Formation|41440|4|Described|p137|||||||||
27407|Flacourt Formation|41445|5|Briefly described|p192|||||||||
27407|Flacourt Formation|41447|6|Mentioned|p227|||||||||
27407|Flacourt Formation|41732|6|Mentioned|p540|||||||||
27407|Flacourt Formation|41751|6|Mentioned|p5|||||||||
27407|Flacourt Formation|42116|5|Briefly described|Fig.1 P6|||||||||
27407|Flacourt Formation|42598|3|Fully described|p92|Valanginian early|late Berriasian|||||||07-FEB-19
27407|Flacourt Formation|42677|6|Mentioned|p19|||||||||
27407|Flacourt Formation|43711|6|Mentioned|Table 4,p28|||||||||
27407|Flacourt Formation|43712|5|Briefly described|p11|||||||||
27407|Flacourt Formation|43722|5|Briefly described|p10|||||||||
27407|Flacourt Formation|43724|5|Briefly described|p29|||||||||
27407|Flacourt Formation|50085|5|Briefly described|p24 Tb. 6|Early Cretaceous|Early Cretaceous|Geological Province: Northern Carnarvon Basin.||||||
27407|Flacourt Formation|64977|6|Mentioned|p493 Fig.3.|Early Cretaceous|Early Cretaceous|Thevenard Island area.||||||
27407|Flacourt Formation|67200|5|Briefly described|p8 fig 6, p54|Cretaceous|Cretaceous|Thermal conductivity of 2.83 W/mK||Barrow Group||Overlies Malouet Formation, unconformably overlain by Mardie Greenstone|Interbedded sandstone and siltstone.|
27407|Flacourt Formation|69689|6|Mentioned|p16|Cretaceous|Cretaceous|Northern Carnarvon Basin.||||||
27407|Flacourt Formation|70066|5|Briefly described|Regional: p6|Early Cretaceous|Early Cretaceous|Barrow Sub-basin, Northern Carnarvon Basin. Oil reservoir.||Barrow Group.||||
25909|Flag Sandstone|24246|6|Mentioned|p19|||Geological Province: Carnarvon Basin.||||||
25909|Flag Sandstone|24315|6|Mentioned|p43|||Associated with the Barrow Group.||||||
25909|Flag Sandstone|24390|5|Briefly described|p24 Table 6|||Geological Province: Northern Carnarvon Basin.||||||
25909|Flag Sandstone|41170|5|Briefly described|p155|||||||||
25909|Flag Sandstone|41438|6|Mentioned|p108|||||||||
25909|Flag Sandstone|41439|6|Mentioned|p116|||||||||
25909|Flag Sandstone|41440|4|Described|p137|||||||||
25909|Flag Sandstone|41445|5|Briefly described|p192|||||||||
25909|Flag Sandstone|41446|6|Mentioned|Fig.2|||||||||
25909|Flag Sandstone|41447|4|Described|p227|||||||||
25909|Flag Sandstone|41454|6|Mentioned|p61|||||||||
25909|Flag Sandstone|41732|6|Mentioned|p540|||||||||
25909|Flag Sandstone|41751|2|Defined|p5|Valanginian|Berriasian|||||||
25909|Flag Sandstone|42395|6|Mentioned|p80|||||||||
25909|Flag Sandstone|42598|3|Fully described|p92|Valanginian|Berriasian|Age latest Berriasian to early Valanginian.||||||01-SEP-08
25909|Flag Sandstone|43712|5|Briefly described|p11|||||||||
25909|Flag Sandstone|43722|5|Briefly described|p10|||||||||
25909|Flag Sandstone|43826|6|Mentioned|Fig.2,p163||Early Cretaceous|||||||01-MAR-10
25909|Flag Sandstone|50085|5|Briefly described|p24 Tb. 6|Early Cretaceous|Early Cretaceous|Geological Province: Northern Carnarvon Basin (Barrow Sub-basin)..||||||
25909|Flag Sandstone|60379|6|Mentioned|p126 fig 3|Valanginian|Valanginian|Dampier sub-basin, Carnarvon Basin||||||
25909|Flag Sandstone|60386|6|Mentioned|p302|Valanginian|Valanginian|Northern Carnarvon Basin. Distal shelf/basin.||||||
25909|Flag Sandstone|62734|5|Briefly described|p1362 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Barrow Sub-basin.||||||01-SEP-08
25909|Flag Sandstone|63950|5|Briefly described|p336 Fig. 4|Valanginian|Valanginian|Geological Province: northern Carnarvon Basin.||||||27-MAY-08
25909|Flag Sandstone|64693|6|Mentioned|p389 |||Barrow Sub-basin. Deep-water mass-flow deposits with diagnostic features including massive sandstone, dish structures, and vertical water escape pillars.||||||
25909|Flag Sandstone|64979|6|Mentioned|pp541-550.|Early Cretaceous|Early Cretaceous|Hydrocarbon reservoir in Barrow Sub-basin.||||||
25909|Flag Sandstone|66126|6|Mentioned|p206|Early Cretaceous|Early Cretaceous|Carnarvon Basin.||||||
25909|Flag Sandstone|67200|6|Mentioned|p17 table 1, p54, p64|||Thermal conductivity of 2.83 W/mK||Barrow Group||||
25909|Flag Sandstone|69689|6|Mentioned|p16|Cretaceous|Cretaceous|Northern Carnarvon Basin.||||Is overlain by Muderong Shale.||
25909|Flag Sandstone|70066|5|Briefly described|Regional: Fig.6; p6|Valanginian|Valanginian|Barrow Sub-basin, Northern Carnarvon Basin. Deposited as a basin-floor fan.||Barrow Group.||Overlies Barrow Group. Is overlain by Muderong Shale and ?locally Zeepaard Formation.||
25909|Flag Sandstone|73564|6|Mentioned|p1232|||North Carnarvon Basin.||||||
28555|Flaggy Member|42080|5|Briefly described|p283|||||||||
27155|Flat Rock Formation|22496|4|Described|p12||Neoproterozoic|Of the Albert Edward Group.  Geological Province: Wolfe Basin.||||||16-AUG-04
27155|Flat Rock Formation|22547|6|Mentioned|p28||Neoproterozoic III|Of the Albert Edward Group.||||||14-NOV-06
27155|Flat Rock Formation|22777|5|Briefly described|Map|||Of theAlbert Edward Group. Geological province:  Wolfe Basin.||||||06-NOV-08
27155|Flat Rock Formation|23621|4|Described|p34|Neoproterozoic|Neoproterozoic|See also page 9 table 1. Of Albert Edward Group. Underlain by Nyuless Sandstone. Geological Province: Wolfe Basin. Max. thickness: >300 m.||||||06-NOV-08
27155|Flat Rock Formation|23622|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Albert Edward Group. Geological Province: Wolfe Basin.||||||
27155|Flat Rock Formation|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|Of Albert Edward Group.||||||
27155|Flat Rock Formation|24173|5|Briefly described|p25|Neoproterozoic|Neoproterozoic|Of the  Albert Edward Group. Overlies the Nyuless Sandstone.||||||06-APR-05
27155|Flat Rock Formation|29813|4|Described|Table 2|||||||||
27155|Flat Rock Formation|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27155|Flat Rock Formation|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
27155|Flat Rock Formation|32660|5|Briefly described|Table 6|||||||||
27155|Flat Rock Formation|32728|6|Mentioned|Table 7|||See also Fig.16||||||
27155|Flat Rock Formation|36532|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
27155|Flat Rock Formation|36551|6|Mentioned|Table 12|||||||||
27155|Flat Rock Formation|36888|4|Described|p214|||||||||
27155|Flat Rock Formation|36898|5|Briefly described|Table II|||||||||
27155|Flat Rock Formation|37927|6|Mentioned|Fig.2|||||||||
27155|Flat Rock Formation|38157|6|Mentioned|Table X|||||||||
27155|Flat Rock Formation|41429|6|Mentioned|p248|||||||||
27155|Flat Rock Formation|43299|5|Briefly described|Map Legend||Neoproterozoic|Of Albert Edward Group.||||||06-NOV-08
27155|Flat Rock Formation|43300|5|Briefly described|Map Legend||Neoproterozoic|||||||
27155|Flat Rock Formation|43301|5|Briefly described|Map Legend||Neoproterozoic|Of Albert Edward Group.||||||06-NOV-08
27155|Flat Rock Formation|43303|5|Briefly described|Map Legend||Neoproterozoic|Of Albert Edward Group.||||||06-NOV-08
27155|Flat Rock Formation|44140|5|Briefly described|p301 fig 4-7, p302 Tb.4-2|Neoproterozoic|Neoproterozoic|Osmond Range (East Kimberley) area. 30 m thick.||Of Albert Edward Group.||Overlies Nyuless Sandstone conformably.|Purple shale, interbedded dolomitic sandstone and quartz sandstone.|07-MAR-18
27155|Flat Rock Formation|44324|14|Not recorded|p.10||Adelaidean|Tb.2. (Adelaidean).||||||
27155|Flat Rock Formation|44325|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
27155|Flat Rock Formation|45047|2|Defined|p97|Adelaidean|Adelaidean|Described p36.||||||06-NOV-08
27155|Flat Rock Formation|45140|3|Fully described|p13, p59-60, Appx.p39|||Dow and Gemuts (1969). Unnamed basin NW of Birrindudu Basin. Named after Flat Rock Yard. [No type section details]. 600m to probably over 1000m thick. No fossils known.||Topmost Albert Edward Group.||Conformably overlies Nyuless Sandstone or Timperley Shale. Is overlain unconformably by Antrim Plateau Volcanics.|Poorly sorted and partly pebbly sublithic arenite, thinly interbedded mauve micaceous siltstone and shale, thin-bedded to laminated siltstone, and ripple-marked fine-grained sublthic arenite. Locally capped by laterite.|
27155|Flat Rock Formation|48927|6|Mentioned|Table 1|||Refers Dow & Gemuts (1969)||||||
27155|Flat Rock Formation|63458|6|Mentioned|p873 Fig.2, p897 Fig.19. |Ediacaran|Ediacaran|||Unit in Albert Edward Group.||||
27155|Flat Rock Formation|64104|6|Mentioned|p62 fig.1, p71 Tb. 2, p72 Fig.8|Neoproterozoic|Neoproterozoic|||Of Albert Edward Group.||Overlies Nyuless Sandstone.||18-MAY-15
27155|Flat Rock Formation|67484|6|Mentioned|p294, p295 Fig.2|Ediacaran|Ediacaran|East Kimberley.||Of the Albert Edward Group.||Overlain by the Antrim Plateau Volcanics. Underlain by the Nyuless Sandstone.||
27155|Flat Rock Formation|67620|5|Briefly described|p5|Ediacaran|Ediacaran|East Kimberley region.||Albert Edward Group.||Overlies Nyuless Sandstone. Is overlain by Antrim Plateau Volcanics.||
27155|Flat Rock Formation|68138|6|Mentioned|p153, 156|Neoproterozoic|Neoproterozoic|East Kimberley region.||Albert Edward Group.||||
27155|Flat Rock Formation|68244|4|Described|p660|Neoproterozoic|Neoproterozoic|East Kimberly area, Kimberley region.||Unit of Albert Edward Group.||Uppermost unit of Albert Edward Group. Underlain by Nyuless Sandstone.||
27155|Flat Rock Formation|68473|6|Mentioned|p529, 531-534, p536, p546-547|Ediacaran|Ediacaran|||Albert Edward Group||Overlies the Timperley Shale. Equivalent to the Rawnsley Quartzite.||
27155|Flat Rock Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Wolfe Creek Basin||Of Albert Edward Group.|||Glacigenic purple micaceous shale and siltstone, with interbedded fine- to coarse-grained sandstone, pebbly and locally dolomitic.|31-JUL-15
27155|Flat Rock Formation|69165|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran||||||Glacigenic purple micaceous shale and siltstone, with interbedded fine to coarse grained sandstone, pebbly and locally dolomitic.|
27155|Flat Rock Formation|69634|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1.|635-541 Ma (Inferred)|Unit of Albert Edward Group.|||Glacigenic purple micaceous shale and siltstone, with interbedded fine- to coarse-grained sandstone, pebbly and locally dolomitic|
27155|Flat Rock Formation|70154|4|Described|100k_interpgeop_lut.csv|Fortunian|Ediacaran||541-635 Ma|Albert Edward Group|||Glaciogenic micaceous shale and siltstone with interbedded fine to coarse grained sandstone, pebbly and locally dolomitic.|
27155|Flat Rock Formation|71267|4|Described|GEOL_LUT_CSV files|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|635-541 Ma (inferred)|Unit of Albert Edward Group.|||Glacigenic purple micaceous shale and siltstone, with interbedded fine- to coarse-grained sandstone, pebbly and locally dolomitic|
68675|Flat Rocks Tonalite|63372|4|Described|Map Legend|Archean|Archean|Of the Yule Granitoid Complex. Age: 3165Ma. Geological Province: East Pilbara Granite-Greenstone Terrane. Biotite bearing tonalite; strongly foliated; interleaved with massive to weakly foliated, K-feldspar porphyritic monzogranite; metamorphosed||||||07-NOV-08
68675|Flat Rocks Tonalite|63441|2|Defined|p35, p9 Tb. 2|Archean|Archean|Of the Mount Billroth Supersuite. Unconformably overlain by Fortescue Group. Ages: 3166+/-5Ma and 3164+/-4Ma. Geological province: East Pilbara Terrane/Pilbara Craton.||||||07-FEB-11
68675|Flat Rocks Tonalite|66118|5|Briefly described|p147|||Pilbara Craton. East Pilbara Terrane.|c. 3165 Ma emplacement age, Nelson 2000b,c|||Igneous||
68675|Flat Rocks Tonalite|66302|6|Mentioned|p84|Mesoarchean|Mesoarchean|Ages derived from Van Kranendonk et al. (2006).|3166 +/- 5 Ma, 3164 +/- 4 Ma |||||
68675|Flat Rocks Tonalite|70775|6|Mentioned|p70||||c. 3165 Ma|||||
68675|Flat Rocks Tonalite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||tonalite|
68675|Flat Rocks Tonalite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||Max age 3166+/-5 Ma, min 3164+/-4 Ma.|Mount Billroth Supersuite|||Biotite metatonalite, strongly foliated and interleaved with K-feldspar porphyritic monzogranite.|
68675|Flat Rocks Tonalite|72668|6|Mentioned|p10|||Western margin of the East Pilbara.|c. 3170 Ma|Mount Billroth Supersuite||||
81847|Flat Top Limestone|72505|5|Briefly described|p890|Artinskian|Artinskian|Southeast Southern Bonaparte Basin. Correlated with the Striatopodocarpites fusus zone.||||Unconformably overlies the Keyling Formation. Overlain by the Fossil Head Formation.||04-MAR-20
81847|Flat Top Limestone|73117|6|Mentioned|p15|Artinskian|Artinskian|Bonaparte Basin, southern.||||Overlain and equivalent to Fossil Head Formation.||
75708|Fleece Pool Gabbro|66195|5|Briefly described|p608-609, p611 Fig.9|Neoarchean|Neoarchean|Of Yalgowra Suite (see sample 185922 p606). ?intrudes the Polelle Group. See other references to sample 185922 p607.|Age: 2735 +/- 5 Ma (Pb/Pb SHRIMP zircon).|||||13-MAR-12
75708|Fleece Pool Gabbro|67129|5|Briefly described|p55|Archean|Archean|Northern Murchison Domain, Youanmi Terrane.|2735 +/- 5 Ma.|||||
75708|Fleece Pool Gabbro|68107|6|Mentioned|p618|Neoarchean|Neoarchean|Western Youanmi Terrane.|2735 +/- 5 Ma (Ivanic et al. 2010).|||||
75708|Fleece Pool Gabbro|68561|4|Described|GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. Mafic Sill. The U-Pb zircon age of 2735 +/- 5 Ma interpreted as the igneous crystallization age of the gabbro sill. Relationships, age from Geochron file 185922.1.pdf.||Yalgowra Suite|||Leucogabbro sill|
75708|Fleece Pool Gabbro|69583|5|Briefly described|p49|Neoarchean|Neoarchean|Murchison Domain.||Yalgowra Suite.||||
75708|Fleece Pool Gabbro|69584|5|Briefly described|p5 Fig.2|Neoarchean|Neoarchean|||Yalgowra Suite|||Gabbro.|
75708|Fleece Pool Gabbro|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Yalgowra Suite.||||
75708|Fleece Pool Gabbro|70796|6|Mentioned|185921.1.pdf|||Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Yalgowra Suite|||Mafic sill of coarse grained to pegmatoidal leucogabbro.|
75708|Fleece Pool Gabbro|70830|5|Briefly described|p27-p28|||Murchison Domain.||||||
75708|Fleece Pool Gabbro|71168|5|Briefly described|p7, p25|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|2735 +/- 5 Ma (Wingate et al., 2010a)|Yalgowra Suite|||Leucogabbro sill.|
75708|Fleece Pool Gabbro|71269|5|Briefly described|185911.1.pdf|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.||Unit of Yalgowra Suite.||||
75708|Fleece Pool Gabbro|73596|6|Mentioned|p1165, 1167, 1170|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane.|2735 +/- 5 Ma.|Yalgowra Suite.||Separates Polelle and overlying Glen Groups.||
35835|Fletcher Creek Granite|23323|5|Briefly described|p456 Tb. 1, p457 Fig. 4|Orosirian|Orosirian|Age: 1850+/-2Ma. Includes garnet-bearing leucocratic sills.||||||07-FEB-07
35835|Fletcher Creek Granite|23568|6|Mentioned|p2777 Fig 2|||||||||
35835|Fletcher Creek Granite|23925|5|Briefly described|p221 Table 1|Orosirian|Orosirian|Age: 1850 +/- 2 Ma. Geological Province: Halls Creek Orogen.||||||
35835|Fletcher Creek Granite|60533|5|Briefly described|p593 Fig. 2, 594|Paleoproterozoic|Paleoproterozoic|Geological Province: Halls Creek Orogen. Age: 1850 +/- 2Ma.||||||07-NOV-08
35835|Fletcher Creek Granite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Tickalara Metamorphics|||Foliated leucocratic biotite-muscovite(-garnet-magnetite) metamonzogranite; rounded to angular inclusions of amphibolite and country rock.|31-JUL-15
35835|Fletcher Creek Granite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Foliated leucocratic biotite--muscovite(--garnet--magnetite) metamonzogranite; rounded to angular inclusions of amphibolite and country rock.|
35835|Fletcher Creek Granite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Central Zone.|1850-1850 Ma (Isotopic)|Unit of Tickalara Metamorphics.|||Foliated leucocratic biotite-muscovite(-garnet-magnetite) metamonzogranite; rounded to angular inclusions of amphibolite and country rock|
35835|Fletcher Creek Granite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1849 Ma||||Foliated leucocratic biotite-muscovite metamonzogranite, rounded to angular inclusions of amphibolite.|
35835|Fletcher Creek Granite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1850+\-2 Ma (isotopic)|Unit of Tickalara Metamorphics.|||Foliated leucocratic biotite-muscovite(-garnet-magnetite) metamonzogranite; rounded to angular inclusions of amphibolite and country rock|
23595|Flores Member|42598|3|Fully described|p98|late Valanginian|middle Valanginian|Reserved.||||||
75624|Fly Dam Formation|67888|6|Mentioned|p68|||||||||
75624|Fly Dam Formation|68186|5|Briefly described|p8, p13, p16-17, p19, p36-37, p54 Fig.35|Mesoproterozoic|Paleoproterozoic|See also p55, Plate 1A. Biranup Zone, Kepa Kurl Booya Province. Exposed S of the Trans-Australian Railway. Lithology and deformation described in some detail. Various age determinations described. Metamorphosed at 1196 +/- 13 Ma and 1154 +/- 35 Ma. Initial-Hf plots.|Between 1640 +/- 12 Ma and 1535 +/- 26 Ma.||||A succession of amphibolite- to granulite-facies, interlayered semipelitic to psammitic gneisses with leucosomes; pelitic layers garnet- and biotite-rich.|
75624|Fly Dam Formation|68654|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Barren Basin.|c. 1620 Ma|||||
75624|Fly Dam Formation|69386|5|Briefly described|p4, p6|Proterozoic|Archean|Biranup Zone, Albany-Fraser Orogen.|||||A succession of interbedded psammitic to pelitic gneiss (metamorphosed interbedded sandstones and mudstones).|
75624|Fly Dam Formation|69595|5|Briefly described|p8, p9 fig 5, p10 tbl 2, p13 fig 7a.|Statherian|Statherian|Eastern Biranup Zone. May be part of the younger Arid Basin as opposed to the Barren Basin on the basis of its young maximum depositional ages.May represent the last stage of basin formation. Potentially deposited in a deep marine setting. At least 100m thick. Other ages provided (p10 tbl 2). Ages of inherited detrital zircons also given  (see page 19). See also p14, p15, p17 tbl 3, p18, p19, p32, p34 fig 19, p35, p36, p40, p57.|c. 1617 Ma (maximum depositional age) - 1140 Ma.||||Interbedded sandstone and mudstone (turbidites?), psammitic and pelitic gneisses.|
75624|Fly Dam Formation|70090|4|Described|p443-449,451-453,457-458|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen, West Australian Craton. Of Barren Basin. Depositional environment: deep marine? Thickness: >100m. Deposition occurred in the late stages of, or shortly after, Biranup Orogeny. Inversion related to Zanthus Event (of Biranup orogeny) may had eroded and shed detritus into Barren Basin. Metamorphosed to upper amphibolite to granulite facies, garnet and psammitic gneiss. Maximum depositional age: c 1617 Ma. Minimum depositional age: constrained by 1196+\-13 and 1154+\-35 Ma metamorphism. Detrital zircon Paleoproterozoic age components include c. 1829, 1672 (major), 1640, 1633 and 1617 Ma. Contains c. 1760 to 1640 Ma detrital zircon age component. Also has EHfi array between -5 to 6, corresponding to 2.0-2.7 GA model ages. Paleoproterozoic age components and Hf isotope signatures are closely similar to, and indicate derivation from Biranup Zone magmatic rocks.|||||Interbedded sandstone and mudstone (turbidites?)|
75624|Fly Dam Formation|70153|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|Barren Basin, Albany-Fraser Orogen.|1617 +/- 26 Ma (isotopic) - 1600 Ma (inferred).||||Interbedded psammitic to pelitic gneiss with leucosomes; pelitic garnet- and biotite-rich layers.|
75624|Fly Dam Formation|70182|6|Mentioned|p3-5|Paleoproterozoic|Paleoproterozoic|Barren Basin, Albany-Fraser Orogen.||||||
75624|Fly Dam Formation|70732|4|Described|p285,287,290-294,296,300|||Geological province: Biranup Zone, Albany-Fraser Orogen. Of Barren Basin. Metamorphosed to amphibolite- to granulite-facies. Contains c. 1679 and c. 1672 Ma detritus with Hf isotopic compositions similar to Biranup zone granites. LA-ICPMS titanite geochronology and SIMS zircon U-Pb geochronology presented in this study. Sample 2: LA-ICPMS metamorphic age 1203+\-6 Ma; SIMS U-Pb zircon metamorphic age 1196+\-11 Ma. Sample 3: LA-ICPMS metamorphic age 1153+\-27 Ma; SIMS U-Pb metamorphic zircon age 1154+\-35 Ma (Kirkland et al., 2012). Youngest detrital age: 1685+\-8 Ma (Sample 2), 1640+\-12 Ma (Sample 3). Titanite metamorphic ages reflect rapid cooling after Stage II metamorphism.|||||Interlayered psammitic to semipelitic gneisses.|
75624|Fly Dam Formation|70802|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Geological province: Albany-Fraser Orogen, West Australian Craton. Commonly migmatitic, with prevalent diatexitic textures, and contains both folded and foliation-parallel leucosomes. Events: Albany-Fraser Orogeny Stage I (133-1260 Ma); Albany-Fraser Orogeny Stage II (1225-1140 Ma); Biranup Orogeny (1710-1620 Ma). Sample GSWA 194742 (psammitic gneiss) yielded a weighted mean 207Pb*/206Pb* date of 1640+\-12 Ma, interpreted as a maximum depositional age of the psammite protolith. Sample GSWA 1947423 (pelitic gneiss) yielded a weighted mean 207Pb*/206Pb* date of 1617+\-26 Ma, interpreted as a maximum depositional age of the pelitic protolith. Sample GSWA 194789 (migmatitic paragneiss) yielded a weighted mean 207Pb/206Pb age of 1678+\-7 Ma, interpreted as maximum depositional age of the sedimentary protolith; and a concordia age of 1197+\-11 Ma, interpreted as age of high-grade metamorphism. See 500k_interpgeop14_lut.csv, 250k_pre_mesozoic_interpgeop_lut.csv.|1617+\-26 Ma; 1600 Ma (inferred)||||Interbedded psammitic to pelitic gneiss with leucosomes; pelitic garnet- and biotite-rich layers|
75624|Fly Dam Formation|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Albany-Fraser Orogen, West Australian Craton. Of Barren Basin. Events: Albany-Fraser Orogeny Stage II (1225 - 1140 Ma); Albany-Fraser Orogeny (1330 - 1140 Ma); Albany-Fraser Orogeny Stage I (1330 - 1260 Ma). See 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|1617+\-26 Ma; 1600 Ma (inferred)||||Interbedded psammitic to pelitic gneiss with leucosomes; pelitic garnet- and biotite-rich layers|
75624|Fly Dam Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Barren Basin.|Max age 1617+/-26 Ma, Min ~1600 Ma.||||Interbedded psammitic to pelitic gneiss with leucosomes; pelitic garnet- and biotite-rich layers.|
75624|Fly Dam Formation|72710|6|Mentioned|p8.|||Samples of zircon grains measured for U-Th-Pb, Lu-Hf and O isotopes.|||||Comprising interlayered psammitic and semi-pelitic lithologies.|22-OCT-20
75624|Fly Dam Formation|73084|6|Mentioned|p12, p56|||Albany-Fraser Orogen, Kepa Kurl Booya Province, Biranup Zone and Fraser Zone.||||||
69014|Flying Foam Suite|64174|5|Briefly described|Map legend|Archean|Archean|Includes the Gidley Granophyre.  Age: c.2724Ma.||||||07-NOV-08
69014|Flying Foam Suite|64580|6|Mentioned|map legend|||||||||
69014|Flying Foam Suite|67201|5|Briefly described|p16-17 Fig.9|Archean|Archean|Pilbara Craton. In Roebourne-Karratha area.|||Gidley Granophyre|||
69014|Flying Foam Suite|69185|5|Briefly described|500k_geologyp08_lut.csv|||Geological Province: Pilbara Craton.|||Includes Gidley Granophyre.|||
69014|Flying Foam Suite|70775|5|Briefly described|p15|||Pilbara Craton.|||Includes the Gidley Granophyre.|||
69014|Flying Foam Suite|70826|6|Mentioned|p8|Neoarchean|Neoarchean|Intrudes the western Pilbara Craton.|||Gidley Granophyre|||
69014|Flying Foam Suite|72034|6|Mentioned|500k_interpgeop16_lut|Neoarchean|Neoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Gidley Granophyre.|||
78621|Foal Creek intrusion|63866|5|Briefly described|p133|||Western Zone, Halls Creek Orogen.||||||
78621|Foal Creek intrusion|69099|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|Grouped as Springvale, Wilagee, and Foal Creek intrusions, with a single lith description in 500k_geologyp08_lut.csv.|||||layered mafic-ultramafic intrusions; peridotite, troctolite, gabbro, olivine gabbro, olivine gabbronorite, gabbronorite, leucogabbro, and anorthosite; minor chromitite layers|
78621|Foal Creek intrusion|69634|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Layered mafic-ultramafic intrusions; peridotite, troctolite, gabbro, olivine gabbro, olivine gabbronorite, gabbronorite, leucogabbro, and anorthosite; minor chromitite layers.|
40473|Forest Belle Gabbro|50075|5|Briefly described|p9|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
40473|Forest Belle Gabbro|50076|5|Briefly described|Map|Archean|Archean|Coarse-grained gabbro with clinopyroxene oikocrysts; metamorphosed.  Geological Province: Yilgarn Craton.||||||05-AUG-15
40473|Forest Belle Gabbro|65265|6|Mentioned|p75|||East Ida greenstone belt.||||||
40473|Forest Belle Gabbro|68289|5|Briefly described|p22|||Petrography is described in detail. Strongly foliated near contact with the Copperfield Monzogranite (nature of contact not provided).|||||Distinctive, coarse to very coarse grained metagabbro with very coarse ophitic texture.|
40473|Forest Belle Gabbro|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton|||||Coarse-grained gabbro with clinopyroxene oikocrysts; metamorphosed.|05-AUG-15
40473|Forest Belle Gabbro|69631|5|Briefly described|p36|||Wyche (2004). Typically massive, but strongly foliated near the contact with Copperfield Monzogranite, where it is cut by auriferous gold veins.|||||A distinctive, coarse- to very coarse-grained metagabbro with very coarse ophitic texture. Very coarse oikocrysts of plagioclase may exceed 5cm across. Plagioclase content ranges from typically at least 50% to over 70%.|
40473|Forest Belle Gabbro|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|See also 500k_interpgeop14_lut.csv.|2704 - 2665 Ma (inferred).||||Coarse-grained gabbro with clinopyroxene oikocrysts; metamorphosed.|
40473|Forest Belle Gabbro|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||gabbro|
40473|Forest Belle Gabbro|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma); Eastern Goldfields Superterrane events (2960 - 2600 Ma). See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv.|2704-2665 Ma (inferred)||||Coarse-grained gabbro with clinopyroxene oikocrysts; metamorphosed|
40473|Forest Belle Gabbro|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||||||Coarse-grained gabbro with clinopyroxene oikocrysts; metamorphosed.|
40473|Forest Belle Gabbro|73596|6|Mentioned|p1164|Neoarchean|Neoarchean|Kalgoorlie-Kurnalpi Rift. Mis-spelt as Forrest Belle Gabbro.|2731 +/- 8 Ma (Wingate et al., 2022).|||||
70615|Forestier Bay Granodiorite|63441|5|Briefly described|p37|Archean|Archean|Of the Orpheus Supersuite and within the structure of Harding Granitic Complex. See also the misspelt Forrestier Bay Granodiorite.||||||07-FEB-11
70615|Forestier Bay Granodiorite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Orpheus Supersuite. Geological province: Pilbara Craton. Biotite granodiorite and monzogranite; sparsely porphyrytic; metamorphosed.||||||07-NOV-08
70615|Forestier Bay Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite, monzogranite|
70615|Forestier Bay Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|De Grey Superbasin.|3014+/-3 Ma.|Orpheus Supersuite|||Biotite granodiorite and monzogranite; sparsely porphyritic; metamorphosed.|
23599|Forestier Claystone|12498|6|Mentioned|p517 Fig.3. |Early Cretaceous|Early Cretaceous|||||||
23599|Forestier Claystone|42598|3|Fully described|p89|Valanginian|Berriasian|Age: early Berriasian to early Valanginian||||||
23599|Forestier Claystone|42615|6|Mentioned|p35|||||||||
23599|Forestier Claystone|44937|5|Briefly described|p92||Early Cretaceous|||||||
23599|Forestier Claystone|60379|5|Briefly described|p126 fig 3, p127, 128, p136, 138|Berriasian|Berriasian|Dampier sub-basin, Carnarvon Basin. Marine claystone. Seal for Angel Formation hydrocarbon play.|||Includes Talisman Member|||29-APR-13
23599|Forestier Claystone|60386|6|Mentioned|p302|Valanginian|Berriasian|Northern Carnarvon Basin. Distal shelf/basin.||||||
23599|Forestier Claystone|62837|5|Briefly described|Stratigraphic columns|Late Jurassic|Late Jurassic|Age: 140-135Ma. Geological Province: Barrow and Dampier Sub-basins, Rankin Platform and Beagle Sub-basin, Roebuck Basin and offshore Canning.||||||01-MAR-10
23599|Forestier Claystone|64978|6|Mentioned|p528 Fig.2.|Early Cretaceous|Early Cretaceous|||||||
23599|Forestier Claystone|66126|6|Mentioned|p206|Early Cretaceous|Early Cretaceous|Carnarvon Basin.||||||
23599|Forestier Claystone|67368|5|Briefly described|p209 Fig.4, pp212-213. |Early Cretaceous|Early Cretaceous|Forms a seal, with Muderong Formation, in the Pemberton Field.||||Overlies Angel Formation. Is overlain by Muderong Shale.||
23599|Forestier Claystone|67369|6|Mentioned|p251.|||The top of this unit was used as a seismic marker for interpreting the Pluto Field data. Forms a seal over the Pluto Gas Field.||||||
23599|Forestier Claystone|67970|5|Briefly described|p3.|Early Cretaceous|Early Cretaceous|Exmouth Plateau. A distal equivalent north of the Barrow Group delta lobe.||||||29-APR-13
23599|Forestier Claystone|69689|6|Mentioned|p16|Cretaceous|Cretaceous|Northern Carnarvon Basin.||||Overlies Dingo Claystone. Is overlain by Muderong Shale.||
23599|Forestier Claystone|70066|5|Briefly described|Dampier: Fig.2. Exmouth: Fig.2; p2-3|Valanginian|Berriasian|See also Regional: Fig.6; p9. Northern Carnarvon Basin. Intra-formational claystones have the potential to form stacked reservoirs and intraformational seals.||||Overlies Angel Formation. Is overlain by Muderong Shale and Birdrong Sandstone.||
25914|Forman Sandstone|22754|5|Briefly described|p11 Tb. 3|Mesoproterozoic|Mesoproterozoic|Of the Glidden Group.||||||
25914|Forman Sandstone|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
25914|Forman Sandstone|32660|5|Briefly described|Table 6|||||||||
25914|Forman Sandstone|32728|5|Briefly described|Table 6|||See also P46||||||
25914|Forman Sandstone|36551|6|Mentioned|Table 10|||||||||
25914|Forman Sandstone|36885|4|Described|p180|||||||||
25914|Forman Sandstone|44155|5|Briefly described|p251 Tb.3-11|||65m thick.||Glidden Group|||Quartz sandstone, thick-bedded, well-sorted.|
25914|Forman Sandstone|44231|5|Briefly described|Map Legend|Neoproterozoic||Of the Glidden Group. White, massive to blocky, fine-grained quartz sandstone. geological province: Glidden Basin.||||||26-MAY-05
25914|Forman Sandstone|44397|14|Not recorded|p.10, Table 3||Adelaidean|Glidden Group. Defn. on Tech.File E/52-9.||||||
25914|Forman Sandstone|44398|14|Not recorded|map legend||Adelaidean|||||||
25914|Forman Sandstone|45047|4|Described|p35|||||||||
25914|Forman Sandstone|48927|2|Defined|p9|Adelaidean|Adelaidean|||||||
25914|Forman Sandstone|71267|5|Briefly described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Glidden Group.|||White or purple massive to blocky thickly bedded well sorted fine quartz sandstone|
69949|Forsyths Conglomerate|22769|5|Briefly described|p759|Middle Eocene|Middle Eocene|Described as a 'basal conglomerate' - may therefore be an abbreviated term (Forsyths Conglomerate Member?).  See also Forsyth's Conglomerate.||||||
79567|Fortune Granite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2726-2600 Ma (inferred)||||Granite; metamorphosed|
73861|Forty-Four Hill Member|24391|4|Described|p8-4 Fig.2|Archean|Archean|Of Lizard Hills Formation. Basal conglomerate, well-stratified quartzose sandstone, brownish red sandstone, dolomite, volcanics, chert. Interpreted as a tidal delta deposit. Geological Province: Pilbara Block.||||||07-NOV-08
83115|Four Mile Hill Granite|72485|5|Briefly described|p5|||Kalgoorlie Terrane. Emplaced at the footwall of the Mt Monger Fault.|2613 +/- 11 Ma (Nelson, 1997).||||Low-Ca granite.|
77937|Fourteen Mile Well Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||2820 - 2711 Ma (inferred).||||Psammite and pelite, commonly schistose; local metaconglomerate.|
77937|Fourteen Mile Well Formation|71212|5|Briefly described|intro p2, intro p3|||Yilgarn Craton. ||||Overlies the Satellite Igneous Complex. Overlain by the Songvang Formation.||
77937|Fourteen Mile Well Formation|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2820-2711 Ma (inferred)||||Psammite and pelite, commonly schistose; local metaconglomerate|
77937|Fourteen Mile Well Formation|73151|5|Briefly described|p3|Neoarchean|Neoarchean|Yilgarn Craton. Kalgoorlie Terrane, Agnew Greenstone Belt.||Kalgoorlie Group||Overlies Hickies Bore Basalt, underlies Songvang Formation.|Basalt.|
78597|Fraser Range Metamorphics|65487|3|Fully described|p2 Fig.1, p24, p43-50, p54-58 Figs.27-29|Mesoproterozoic|Mesoproterozoic|Includes the former Fraser Complex of Myers (1985) as well as interlayered metagranitic and metasedimentary rocks previously assigned as undivided Biranup Complex. Part of the Biranup Zone of the Kepa Kurl Booya Province, Albany-Fraser Orogen. Igneous crystallisation c.1287-1291 Ma; high grade mafic and gabbroic rocks  with a strong distinct magnetic/gravity signature; five complex structurally interlayered units described. May represent one or more remnant arcs. Geochronology discussed in great detail.|||||Garnet amphibolite (metagabbro), layered ultramafics, metamelanogabbro, metaleucogabbro, meta-anorthosite, pyroxene granulite, metagabbro, gabbronorite, granulite.|06-AUG-15
78597|Fraser Range Metamorphics|67268|6|Mentioned|p10||||||||Granulite facies metamafic assemblages with interlayered lenses of metagranitic and metasedimentary lithologies.|
78597|Fraser Range Metamorphics|67380|5|Briefly described|p5-6, p11, p22|Ectasian|Ectasian|Fraser Zone, Eastern Albany-Fraser Orogen. Previously interpreted to have been the result of major thrust faults; more recently suggested to be part of a large layered mafic intrusion or remnants of multiple magmatic arcs. Initial Hf isotope ratios are consistent with some additional juvenile input into a reworked Biranup Zone source.|1298 +/- 4 Ma (Kirkland et al., 2011).||||A series of interleaved slivers of granitic gneiss, metasedimentary rocks and mafic gabbroic rocks, now mainly pyroxene granulites.|
78597|Fraser Range Metamorphics|67722|6|Mentioned|p5 fig 2.2, p96|Mesoproterozoic|Mesoproterozoic|Fraser Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen. |c. 1300 Ma(SHRIMP)|||||
78597|Fraser Range Metamorphics|67888|6|Mentioned|p69|||||||||
78597|Fraser Range Metamorphics|68186|4|Described|p7-8, p22-26, p32, p37, p40-41, p48|Mesoproterozoic|Mesoproterozoic|See also p50-55, Plate 1A. Fraser Zone, Kepa Kurl Booya Province. Part of the supracrustal rocks of the Arid Basin. Includes detritus aged c.1407 Ma. Youngest detrital zircon from metasedimentary rocks is 1334 +/- 20 Ma. Typically displays well-developed, NE-trending, steeply-dipping foliation. Strongly mylonitized with folds, faults and shear zones. Probable magma mixing producing hybrids. Lithologies, deformations and geochronology described in detail.|1305-1290 Ma (Spaggiari et al., 2009).||||Mainly sheets of metagabbro rocks interlayered with sheets of granitic material (metamonzogranite to metasyenogranite); and slivers or layers of a variety of pelitic, semipelitic and calcic metasedimentary rocks (granulite facies) of the Arid Basin.|
78597|Fraser Range Metamorphics|68654|4|Described|p3, p5-7|Mesoproterozoic|Mesoproterozoic|Arid Basin, Fraser Zone. Age is age of deposition of sedimentary protoliths, older age is a more conservative estimate. Mafic and felsic magmatism occurred almost immediately afterwards ranging from 1310-1283 Ma. Metamorphism also occurred shortly afterwards, thus deposition, magmatism and metamorphic processes all occurred within a relatively short time frame.|1332+/-21 Ma 1363+/-9 Ma||||Metagabbroic rocks with sheets of metagranitic material and layers of pelitic, semipelitic to calcic metasedimentary rocks.|
78597|Fraser Range Metamorphics|69003|5|Briefly described|p4, p40, p43|Mesoproterozoic|Mesoproterozoic|Albany-Fraser Orogen. Formed by repeated intrusion of gabbroic magma into quartzofeldspathic country rock. Records uplift and associated brittle deformation during the period c.1260-1225 Ma. Hosts Ni-Cu mineralisation at Nova.|1305-1290 Ma.||||Dominantly sheets of metagabbroic rocks, interlayered with sheets of granitic rocks and layers or slivers of pelitic, semipelitic, and calcic metasedimentary rocks of the Arid Basin.|
78597|Fraser Range Metamorphics|69140|4|Described|p1-4, p6,16-18|Ectasian|Ectasian|Geological province: Albany-Fraser Orogen. Northeast-trending suiteof granulite-facies mafic rocks interlayered with metagranites and metasediments. Sedimentary presursors were likely sourced from Paleo-Mesoproterozoic Biranup Zone and deposited in a rapidly developing rift basin c. 1334 Ma. Underwent granulite-facies metamorphism c. 1301+\-6 Ma (Stage 1; Clark et al., 1999) synchronous with emplacement of large volumes of mafic magma in an extensional setting, followed by a HP amphibolite-facies event bracketed in age by the intrusion of 1293 +\- 9 Ma granites and 1288 +\- 12 Ma aplite dykes, 45 Ma of tectonic quiescence and cooled through biotite Rb-Sr closure temperature (300-350deg) between 1270-1260 Ma (Fletcher et al., 1991). Petrography and U-Pb geochronology carried out on samples obtained from Gnamma Hill and Mt Malcolm areas detailed on p4-17.|1305-1290 Ma||||Sheeted and mostly strongly deformed metagabbro and metagranite; sedimentary gneiss - psammitic, semipelitic to pelitic, locally calc-silcate layers, amphibolite-granulite facies gneiss, occasionally iron-rich metasedimentary rocks.|05-JUL-19
78597|Fraser Range Metamorphics|69152|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Fraser Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen|||Includes 13 unnamed subunits.||Mafic gneiss; metagabbro; mafic granulite; felsic granulite; subordinate metagranitic rocks; subordinate garnet-bearing quartzite.|06-AUG-15
78597|Fraser Range Metamorphics|69252|5|Briefly described|p9, p15-16, p19-20|||Spaggiari et al. (2009). Fraser Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen. Arid Basin. Metamorphism around 1304 +/- 7 Ma.|1466 +/- 17 Ma (protolith deposition).||||Mainly metagabbros, interlayered with sheets of granitic material and slivers of pelitic, semipelitic and calcic metasedimentary rocks. Granulite facies metamorphosed, with local regression to amphibolite facies.|
78597|Fraser Range Metamorphics|69386|5|Briefly described|p6|Ectasian|Ectasian|Fraser Zone, Yilgarn Craton.|1.31-1.29 Ga.||||Sheets of metagabbroic rocks interlayered with granitic material and layers of metasedimentary rocks.|
78597|Fraser Range Metamorphics|69595|4|Described|p7, p19, p22, p33, p56|Ectasian|Ectasian|Arid Basin, Fraser Zone. In this study the metasedimentary component is referred to by the alternative name of Snowys Dam Formation. |1305-1290 Ma (Spaggiari et al, 2009)||||Thin to voluminous sheets of metagabbroic rocks interlayered with sheets of metamonzogranitic rocks to metasyenogranitic gneisses and pyroxene-bearing granitic gneiss, and also amphibolite-granulite facies metapelites and metapsammites.|
78597|Fraser Range Metamorphics|69743|6|Mentioned|p190-191|Mesoproterozoic|Mesoproterozoic||1305-1290 Ma.|||||
78597|Fraser Range Metamorphics|70084|5|Briefly described|p220,222|Ectasian|Ectasian|Geological province: Fraser Zone, Albany-Fraser Orogen, Yilgarn Craton. Associated with Stage I (1345-1260 Ma) Albany-Fraser Orogen; coeval with Recherche Supersuite, and correlable to Wankanki Supersuite and Wirku Metamorphics in the western Musgrave Province. A sequence of high-grade metasedimentary rocks in the Arid Basin, intruded by sheets of metagabbro (Fraser gabbro) and metagranite.||||||
78597|Fraser Range Metamorphics|70089|6|Mentioned|p264|Mesoproterozoic|Mesoproterozoic|Fraser Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen.|1305-1290 Ma.||||A sequence of high-grade metasedimentary rocks intruded by sheets of metagabbroic and metagranitic rocks.|
78597|Fraser Range Metamorphics|70090|5|Briefly described|p441-442|Ectasian|Ectasian|Geological province: Fraser Zone, Albany-Fraser Orogen, West Australian Craton. Thin to voluminous sheets of metagabbroic rocks interlayered with sheets of granitic gneisses of the Recherche Supersuite. Intrudes into Snowys Dam Formation, Arid Basin.|1305-1290 Ma|||||
78597|Fraser Range Metamorphics|70094|6|Mentioned|p86|||Albany-Fraser Orogen. MP - HT metamorphism has been attributed to mafic magmatism in a rift-style setting; similar to the scenario in this study of Harts Range Group.||||||
78597|Fraser Range Metamorphics|70153|5|Briefly described|500k_interpgeop14_lut.csv|Mesoproterozoic|Mesoproterozoic|The 1368 +/-12 Ma (SHRIMP) age is derived from psammitic gneiss and mafic granulite samples (194714.1.pdf, 194718.1.pdf) and constrains age of deposition for sedimentary protolith.|1305 +/- 2 Ma - 1287 +/- 14 Ma (isotopic).||||Sheeted and mostly strongly deformed metagabbro, psammitic and semipelitic gneiss, metagranite, and minor metasedimentary rocks; includes hybrid rocks and mafic and felsic granulite.|
78597|Fraser Range Metamorphics|70182|5|Briefly described|p6|||Spaggiari et al. (2009). Fraser Zone, Albany-Fraer Orogen.||||Interbedded with Snowys Dam Formation.|Sheets of metagabbroic rocks, interlayered with sheets of granitic gneiss including pyroxene-bearing granitic gneiss, and hybrid migmatitic rocks; all interlayered with (semi-)pelitic and psammitic gneiss, calc-silicate and iron-rich metasediments.|
78597|Fraser Range Metamorphics|70254|6|Mentioned|p357|||Geological province: Albany-Fraser Orogen.||||||
78597|Fraser Range Metamorphics|70732|6|Mentioned|p285,298-299|Ectasian|Ectasian|Geological province: Fraser Zone, Albany-Fraser Orogen. Metagranite samples yield a mean magmatic crystallization age of c. 1300 Ma. Metamorphism of Fraser Range Metamorphics driven by c. 1300 Ma mafic and felsic magmatism during a granulite facies event at c. 1301+\-6 Ma.|1305-1290 Ma|||||
78597|Fraser Range Metamorphics|70735|6|Mentioned|p29, 33|||Albany-Fraser Orogen. Photographs.|||||Metagabbros, gabbro, metagranites.|
78597|Fraser Range Metamorphics|70802|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Fraser Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen. Events: Albany-Fraser Orogeny Stage II (1225-1140 Ma); Albany-Fraser Orogeny (1330-1140 Ma); Albany-Fraser Orogeny Stage I (1330-1260 Ma). A suite of interleaved, thin slivers of granitic gneiss, metasedimentary rocks, and mafic rocks that are now mostly pyroxene granulites or mafic amphibolites (Myers, 1985; Clark et al., 1999; De Waele and Pisarevsky, 2008). Sample GSWA 183653 (pegmatite) yielded a weighted mean 207Pb*/206Pb* date of 1301+\-6 Ma, interpreted as the magmatic crystallization age of the pegmatite. Sample GSWA 183671 (granitic gneiss) yielded a weighted mean 207Pb*/206Pb* date of 1310+\-7 Ma, interpreted as the magmatic crystallization age of the granitic protolith. Sample GSWA 194714 (psammitic gneiss) yielded a weighted mean 207Pb*/206Pb* date of 1310+\-7 Ma, interpreted as the magmatic crystallization age of the granitic protolith. Sample GSWA 194717 (metagabbro) yielded a concordia age of 1399+\-3 Ma, interpreted as the magmatic crystallization age of the gabbro. Sample GSWA 194718 (mafic granulite) yielded a concordia age of 1291+\-6 Ma, interpreted as age of granulite metamorphism. Sample GSWA 194778 (migmatitic gt-bt gneiss) yielded a weighted mean 207Pb*/206Pb* date of 1363+\-9 Ma, interpreted as maximum depositional age of the sedimentary protolith. Sample GSWA 194779 (metagranite) yielded a weighted mean 207Pb*/206Pb* date of 1293+\-8 Ma, interpreted as maximum depositional age of the sedimentary protolith. Sample GSWA 194780 (granite pegmatite) yielded a concordia date of 1283+\-7 Ma, interpreted as crystallisation age of the pegmatite, synchronous with HT metamorphism. See 100k_geologyp10_lut.csv, 500k_interpgeop14_lut.csv, 250k_pre_mesozoic_interpgeop_lut.csv.|1334+\-20 Ma; 1305+\-2 Ma; 1287+\-14 Ma||||Mafic gneiss, gabbro and granulites, subordinate metagranitic rocks.|
78597|Fraser Range Metamorphics|70826|6|Mentioned|p10|Mesoproterozoic|Mesoproterozoic|||||||
78597|Fraser Range Metamorphics|71270|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Fraser Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage II (1225 - 1140 Ma); Albany-Fraser Orogeny (1330 - 1140 Ma); Albany-Fraser Orogeny Stage I (1330 - 1260 Ma). De Waele and Pisarevsky (2008) reported magmatic crystallization of a gabbro within the Fraser Zone, dated at 1291+\-8 Ma using U-Pb analyses on zircon. Sample GSWA 194714 (psammitic gneiss) yielded a weighted mean 207Pb/206Pb age of 1334+\-20 Ma, interpreted to be maximum depositional age of psammite. Sample GSWA 194715 (leucosome in psammitic gneiss) yielded a concordia age of 1285+\-7 Ma, interpreted as the age of leucosome crystallization, and also of migmatization of this rock. Sample GSWA 194718 (mafic granulite) yielded a concordia age of 1292+\-6 Ma, interpreted to be age of granulite metamorphism. See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|1310+\-7 Ma; 1283+\-7 Ma||||Felsic and mafic granulites; orthopyroxene rich, olivine-bearing, magnetite rich; metagranitic (subordinate mylonitised) with garnet-abundant metagranitic layers, mafic gneiss, metagabbro.|
78597|Fraser Range Metamorphics|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Fraser Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen.|Max age 1310+/-7 Ma, Min 1283+/-7 Ma.|Ungrouped.|||Sheeted and mostly strongly deformed metagabbro, metagranite, and minor metasedimentary rocks; includes hybrid rocks and mafic and felsic granulite.|
78597|Fraser Range Metamorphics|72059|5|Briefly described|p57|Ectasian|Ectasian|Geological province: Fraser Zone, Albany-Fraser Orogen. Of Arid Basin. Protoliths include interlayered metasediment, metagabbro and metagranite, and metamorphosed to upper amphibolite to granulite facies at 1334-1280 Ma during Stage I Albany-Fraser Orogen.||||Interleaved with Recherche Supersuite.||
78597|Fraser Range Metamorphics|72710|6|Mentioned|p19.|||Includes mafic magmatic components.|||||Includes metamorphics.|
78597|Fraser Range Metamorphics|73084|6|Mentioned|p21, p56|||Fraser Zone.||||||
78597|Fraser Range Metamorphics|73597|6|Mentioned|p1178|Mesoproterozoic|Mesoproterozoic|Fraser Zone, Albany-Fraser Orogen.|1305-1290 Ma.|||||
81345|Fraser gabbro|70084|5|Briefly described|p222-223,225,228|Ectasian|Ectasian|Geological province: Fraser Zone, Albany-Fraser Orogen, Yilgarn Craton. Mafic magmatic intrusion within the Fraser Range Metamorphics. ENdi values of -3.42 to -0.35. Considered the most radiogenic component of the Recherche Supersuite.|c. 1300 Ma|Unit of Recheche Supersuite.|||Mettagabbro sheets.|
81345|Fraser gabbro|70735|6|Mentioned|p29, 43 Fig.18|||Dominates the Fraser Zone, Albany-Fraser Orogeny. Th/La, Pb/Zr, Pb/La binary variation diagrams.||||Intrudes Snowys Dam Formation.|Voluminous sheets of metagabbro; olivine gabbronoritic, noritic, and peridotitic cumulates containing Ni-Cu sulphides.|
40071|Frederick Suite|23809|5|Briefly described|p3 Fig. 1|||Same unit as Mount Frederick Suite?  Medium to fine grained, weakly porphyritic to equigranular, foliated to massive biotite monzogranite, hornblende-biotite granodiorite; trondjhemite.||||||22-DEC-08
40071|Frederick Suite|50315|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Biotite hornblende granodorite. I-type; medium to coarse, grey, oval plutons. Age: ~1800Ma.||||||07-NOV-08
40071|Frederick Suite|50374|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Biotite hornblende granodiorite.||||||07-NOV-08
40071|Frederick Suite|50376|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Biotite hornblende granodiorite.||||||07-NOV-08
40071|Frederick Suite|60676|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Biotite hornblende granodiorite: I-type, medium to coarse, grey, oval plutons; strong magnetic response.||||||07-NOV-08
40071|Frederick Suite|61246|6|Mentioned|p30|||Includes the "Pipeline granodiorite".||||||
40071|Frederick Suite|61861|5|Briefly described|p4, 25, Fig 2, Fig.38,  Map 1|Orosirian|Orosirian|Granite suite in Tanami Region, close to WA border. Ovoid, smaller diameter than Coomarie Suite, I-type plutons with high magnetic response. Age inferred from intrusive relationships.|1830 - 1810 Ma.|||||03-APR-12
40071|Frederick Suite|62580|4|Described|p39, p11 Tb. 1, p12 Fig. 2, p69|Paleoproterozoic|Paleoproterozoic|Includes MacFarlanes Peak and Walnut Granodiorites, Nora Range Monzogranite. I-type. Granite plutons of med.- to coarse-gr., equigr., granophyric to porphyritic, leucocratic qtz syenite, biotite-hornblende monzogranite + hornblende-biotite granodiorite.||||||07-FEB-11
40071|Frederick Suite|62628|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Tanami Inlier. Medium to fine grained, equigranular biotite or hornblende bearing monzogranite to syenogranite.||||||07-NOV-08
40071|Frederick Suite|63261|4|Described|p9 Fig. 5, p16|Paleoproterozoic|Paleoproterozoic|Includes the magnetic parts of Browns Range and Coomarie granite suites. Interpreted crystallisation age range: 1815+/-4 to 1801+/-4Ma. Geological province: Tanami Region. Typically medium- to fine-gr. equigranular biotite monzogranite to syenogranite.||||||10-DEC-12
40071|Frederick Suite|64662|5|Briefly described|p30 Fig. 3|Statherian|Orosirian|Age: 1825-1790Ma. Geological Province: Tanami region.||||||07-FEB-11
40071|Frederick Suite|64675|6|Mentioned|Map 1|Paleoproterozoic|Paleoproterozoic|||||||
40071|Frederick Suite|64733|5|Briefly described|p170 Fig.2, p172 Fig.4, p175|Statherian|Orosirian|Moderate to high aeromagnetic response. Spelling error on Fig.2 ('Fredrick Suite')|1815-1790 Ma.|||||20-APR-12
40071|Frederick Suite|65323|5|Briefly described|Map legend|Statherian|Orosirian|Intrusive biotite hornblende granodiorite; I-type; moderate-highly magnetic, low gravity response. Shown as equivalent age to Borefield Road Suite and Granites Suite.||||||18-FEB-13
40071|Frederick Suite|65324|6|Mentioned|Map legend|Statherian|Orosirian|Not shown on map||||||
40071|Frederick Suite|65326|6|Mentioned|Map legend|Statherian|Orosirian|Not shown on map||||||02-FEB-10
40071|Frederick Suite|65327|6|Mentioned|Map legend|Statherian|Orosirian|Not shown on map||||||
40071|Frederick Suite|65328|6|Mentioned|Map legend|Statherian|Orosirian|Not shown on map||||||
40071|Frederick Suite|65349|6|Mentioned|Map legend|Statherian|Orosirian|Not shown on map||||||
40071|Frederick Suite|65350|6|Mentioned|Map legend|Statherian|Orosirian|Not shown on map||||||
40071|Frederick Suite|65351|6|Mentioned|Map legend|Statherian|Orosirian|Not shown on map||||||
40071|Frederick Suite|65352|5|Briefly described|Map legend|Statherian|Orosirian|Intrusive biotite hornblende granodiorite; I-type; moderate-highly magnetic, low gravity response.  Shown as equivalent in age to Granites Suite and Bore Field Road Suite.||||||12-DEC-12
40071|Frederick Suite|65353|5|Briefly described|Map legend|Statherian|Orosirian|Intrusive biotite hornblende granodiorite; I-type; moderate-highly magnetic, low gravity response. Shown as equivalent in age to Granites Suite and Bore Field Road Suite.||||||12-DEC-12
40071|Frederick Suite|65354|6|Mentioned|Map legend|Statherian|Orosirian|Not shown on map||||||
40071|Frederick Suite|65355|6|Mentioned|Map legend|Statherian|Orosirian|Not shown on map||||||
40071|Frederick Suite|65356|6|Mentioned|Map legend|Statherian|Orosirian|Not shown on map||||||
40071|Frederick Suite|65358|5|Briefly described|p6-7|Statherian|Orosirian|In Tanami Region. Dominated by metaluminous I-type biotite granodiorite and monzogranite. Intruded between 1825-1790 Ma.||||||
40071|Frederick Suite|65359|5|Briefly described|p23, p26-28 Figs.26-28.|||Tanami Region. Felsic plutons with high magnetic signature.||||||
40071|Frederick Suite|66129|5|Briefly described|p213, p214 Fig.1, p215 Fig.2|Statherian|Orosirian|1815-1790 Ma. Medium to fine grained, equigranular biotite monzogranite to syenogranite. Accessory minerals of titanite, magnetite, ilmenite, pyrite, apatite and zircon.||||||
40071|Frederick Suite|67168|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|I-type. Low gravity response; variably magnetic.||||Intrudes MacFarlane Peak and Tanami Groups.|Biotite-hornblende granodiorite.|
40071|Frederick Suite|68474|6|Mentioned|p572|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen.|1815-1790 Ma|||||
40071|Frederick Suite|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleoproterozoic|Paleoproterozoic|See also 100k_maginterpgeop_lut.csv. Granites-Tanami Complex.|c.1815-1790 Ma (Huston et al., in press).|Granites Supersuite|Includes Balwina, Lewis, Slatey Creek Granites.||Granite, diorite, gabbro.|
40071|Frederick Suite|69003|5|Briefly described|p5, p17 Fig.21|||Granites-Tanami Orogen.|1820-1790 Ma.|||||
40071|Frederick Suite|69253|5|Briefly described|p755-756, p761, p763, p765|Statherian|Orosirian|Petrophysical properties detailed. Appears in Fig. 1 as Fredrick Suite.|c.1815-1790 Ma.||Includes Balwina, Lewis and Selby Granites.|||
40071|Frederick Suite|69417|5|Briefly described|p2:5|Orosirian|Orosirian|Tanami Region.||||Intrudes Ware Group.||12-JUL-16
40071|Frederick Suite|69426|5|Briefly described|p11:4 Fig.11.3, 11:10-12|Statherian|Orosirian|Comprises several un-named granite plutons which have a distinctive moderate to highly magnetic response, but a low gravity response. Hosts a porphyry gold style deposit at the Buccaneer prospect. Geochemistry briefly described.|1815-1778 Ma.||||Typically medium- to fine-grained, equigranular, biotite monzogranite to syenogranite.|12-JUL-16
40071|Frederick Suite|69432|6|Mentioned|p17:2|||||||Is overlain unconformably by the Birrindudu Group.||12-JUL-16
40071|Frederick Suite|69673|6|Mentioned|p3|||||||||
40071|Frederick Suite|69747|5|Briefly described|p263-p264|Statherian|Orosirian|Geological province: Tanami Block, North Australian Craton. Associated with late syn- to postcollisional tectonic settings within a ~30 Ma million year long period of magmatic activity broadly spanning ca. 1825-1791 Ma (Smith, 2001).|ca. 1815-1790 Ma|||||25-JUN-19
40071|Frederick Suite|70291|4|Described|p178,180-181|Statherian|Orosirian|Geological province: Tanami. Affected by D4 event (ESE-trending crenulations; angular folding late syn- to post-granite intrusion). Inferred to have a deeper source.|1815-1790 Ma||||Magnetic, peraluminous biotite monzogranite to syenogranite with hornblende in SiO2-poorer samples.|
40071|Frederick Suite|70478|4|Described|p2 Fig 1, p3-5, p39 App 3|Statherian|Orosirian|Geological Province: Tanami. Granites drilled in drillholes TAN99DDH1, TAN99DDH2, TAN99DDH3 assigned to Frederick Suite. See associated drilling summaries and appendices for more detail. SHRIMP U-Pb magmatic zircon ages of 1802+\-4 Ma (DDH1 granite; Cross et al., 2005); 1801+\-4 Ma (DDH2 granite; Smith 2001); 1815+\-4 Ma (DDH3 granodiorite; Smith 2001).||||Intrudes Killi Killi Formation, Mount Charles Formation.|monzogranite, syenogranite|
40071|Frederick Suite|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region. Shown in the Cross Section only.|1815-1778 Ma.||||Medium- to fine-grained, equigranular biotite- or hornblende-bearing monzogranite to syenogranite.|
40071|Frederick Suite|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.|1815-1778 Ma.||||Biotite +/- hornblende monzogranite to syenogranite: medium- to fine-grained, equigranular.|
40071|Frederick Suite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||syenogranite, monzogranite|
40071|Frederick Suite|71349|5|Briefly described|p724-725|Paleoproterozoic|Paleoproterozoic|Tanami Region.|1825-1790 Ma.|||Intrudes Tanami and Ware Groups.||
40071|Frederick Suite|73089|5|Briefly described|p3, p8, p39|Statherian|Orosirian|Granites-Tanami Orogen, widespread. Broadly coeval with other granites of the orogen but distinguished by differences in magnetic character (Ahmad et al., 2013).|1815-1778 Ma||Lewis Granite ,Balwina Granite||Medium- to fine-grained, equigranular, biotite monzogranite to syenogranite characterized by relatively strong magnetization.|
40071|Frederick Suite|73158|5|Briefly described|p2|Statherian|Orosirian|Granites-Tanami Orogen.|1815-1778 Ma||||Granitic intrusions.|
40071|Frederick Suite|73159|5|Briefly described|p2|||Granites-Tanami Orogen.|1815-1778 Ma.||||Granites.|
33664|Friday Monzogranite|44203|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
33664|Friday Monzogranite|69152|6|Mentioned|1m_geologyp08_lut.csv|Archean|Archean||||||Monzogranite.|06-AUG-15
33664|Friday Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
33664|Friday Monzogranite|71270|5|Briefly described|1m_geologyp12_lut.csv|||Geological province: Yilgarn Craton, West Australian Craton. |||||Monzogranite|
27270|Frigate Shale|13194|4|Described|p385 Tb. 4-16, p396 fig 4-60|Tithonian|Oxfordian|Type section Petrel 1 well (1571-1820m).||Flamingo Group||Overlies Plover Formation (unconformably). Overlain by Sandpiper Sandstone (conformably).|Shale, calcareous shale; minor glauconitic sandstone.|
27270|Frigate Shale|13234|5|Briefly described|p260, p263 Tb.4.|||Important source rock unit.||Of the Flamingo Group||||
27270|Frigate Shale|22663|6|Mentioned|NT97 -1-4 p3|||Of the Flamingo Group.||||||19-SEP-06
27270|Frigate Shale|24047|5|Briefly described|p13|Jurassic|Jurassic|Geological Province: Money Shoal Basin.||||||
27270|Frigate Shale|24569|5|Briefly described|p248 Fig. 3|Tithonian|Kimmeridgian|Of the Flamingo Group. Age: >140Ma. Geological Province: Petrel Sub-basin.||||||02-MAR-05
27270|Frigate Shale|41459|6|Mentioned|Fig.2|||||||||
27270|Frigate Shale|41532|6|Mentioned|p305|||||||||
27270|Frigate Shale|41731|6|Mentioned|Fig.3|||||||||
27270|Frigate Shale|42442|2|Defined|p25|Tithonian|Oxfordian|Same as Frigate Shale in WA.||||||19-SEP-06
27270|Frigate Shale|43661|6|Mentioned|Fig.3|||||||||
27270|Frigate Shale|43699|6|Mentioned|Fig.6,p10||Late Jurassic|||||||
27270|Frigate Shale|43739|6|Mentioned|Fig.5,p38|Late Cretaceous|Late Jurassic|||||||
27270|Frigate Shale|43829|5|Briefly described|Fig.2,p225|Early Cretaceous|Middle Jurassic|||||||
27270|Frigate Shale|49637|5|Briefly described|p7|Early Cretaceous|Late Jurassic|Of the Flamingo Group. Geological Province: Sahul Platform and Petrel Sub-basin.||||||07-FEB-11
27270|Frigate Shale|60386|6|Mentioned|p302|Oxfordian|Oxfordian|Bonaparte Basin. Distal shelf/basin.||||||
27270|Frigate Shale|62837|5|Briefly described|Stratigraphic columns|Late Jurassic|Late Jurassic|Of the Flamingo Group. Age: ~156-~142Ma. Geological Province: Northern Bonaparte Basin and Petrel Sub-basin.||||||09-NOV-06
27270|Frigate Shale|64695|6|Mentioned|p268 Fig.13|||||||||
27270|Frigate Shale|64696|6|Mentioned|p134|Oxfordian|Oxfordian|See also references to Frigate Formation (p125, p126, p127 Fig.2, p131, p134, p138, p140 ). Vulcan Sub-basin. Appears as Frigate Shale (Lower Vulcan Formation). About 1000 m thick.||||||
27270|Frigate Shale|67195|5|Briefly described|Appendix 2|||Bonaparte Basin.|||||Includes grey shale.|
27270|Frigate Shale|67200|6|Mentioned|app 2 p8||||||||Shale.|
27270|Frigate Shale|68135|5|Briefly described|p51 fig 2a|Early Cretaceous|Middle Jurassic|Bonaparte Basin.||Flamingo Group.||Is overlain by Swan Formation.||14-SEP-17
27270|Frigate Shale|69452|5|Briefly described|p36:8, 15, 21-22|||Petrel Sub-basin, Bonaparte Basin. Thickness up to 250m.||Flamingo Group.||Overlies Elang Formation. Is overlain by Sandpiper Sandstone.|Marine mudstone.|12-JUL-16
27270|Frigate Shale|69653|5|Briefly described|p1, 6, 8, 10, p13 Fig.2.4, p15, 37, 39|Late Jurassic|Late Jurassic|Petrel Sub-basin. The lower part is suitable as a reservoir, and the upper part as a seal, for CO2 storage in Elang and Plover Formations. Middle shoreface - offshore deposits. Schematic (gamma ray) well sections. Composite well diagram. Photomicrographs. See also p41-43, 45, 47-49, 51, 53, 59, 63, 68, 73-74, 76. See also references to Frigate Formation (p26-27, 50).||Flamingo Group.||Disconformably overlies Elang Formation. Is overlain by Sandpiper Sandstone.|Sandstone-dominated lower part overlain by mudstone-dominated upper part: bioturbated fine-grained sandstone, bioturbated siltstone with shell fragments, mudstone. Facies described in detail.|
27270|Frigate Shale|69673|6|Mentioned|p173|||||Flamingo Group||||
27270|Frigate Shale|70061|5|Briefly described|Regional geology p6, p12, p14|Valanginian|Oxfordian|Gas- and oil-prone source rocks. Claystones also provide an additional top seal. See also Fig 6 which shows Frigate Shale as Oxfordian to Valanginian, and shown in Upper and Lower parts with time break between in the Laminaria/Flamingo High area and Troubadour Terrace/Sahul Platform area, but no time break in Flamingo/Sahul Syncline or Calder and Malita Graben areas.|||||Marine sediments including mudstones.|18-SEP-18
81346|GMS Suite|70084|4|Described|p222-223,225,228|Ectasian|Ectasian|Geological province: Albany-Fraser Orogen, Yilgarn Craton. Informally nomenclature used to describe the voluminous granodiorite-monzogranite-syenogranite suite that dominates the Nornalup Zone. Felsic; expanded silica range from 60.5 to 76.8 wt.% and are generally calc-alkalic and weakly ferroan (Smithies et al., 2014b). ENdi values of -8.38 to -3.4. Igneous zircons with EHfi values of 0 to -6. Syenogranites closest to Rodona Shear Zone have geochemical and isotopic signatures reflecting reworking of Madura Province crust, in contrast with younger syenogranites immediately to the west showing reworked Archean crustal signatures. Systematic NW-ward decrease in intrusive age from c. 1330 to c. 1283 Ma, corresponding to increasingly primitive compositions (from syenogranite to granodiorite) and changes in isotopic composition reflecting an increase in the source ratio of mantle and reworked Archean crustal material.|c. 1330 Ma|Unit of Recherche Supersuite.|||Granodiorite, monzogranite, syenogranite.|
25917|Gabba Gabba Member|1943|5|Briefly described|p377, p379 Fig.8|||At base of Unit 4, Tumblagooda Group. Has magnetic reversal at base.|||||Pebbly sandstone and pebbly conglomerate.|
25917|Gabba Gabba Member|23726|5|Briefly described|p17|||Geological Province: Carnarvon Basin.||||||
25917|Gabba Gabba Member|42116|5|Briefly described|p11|||||||||
25917|Gabba Gabba Member|42441|2|Defined|p49|Silurian|Silurian|of Tumblagooda Sandstone. Part of Facies Association 3.||||||
25917|Gabba Gabba Member|42715|4|Described|p1015|||||||||
25917|Gabba Gabba Member|61811|5|Briefly described|p11, p13, p17. |Ordovician|Ordovician|Extends along the coastal gorges in the south, about 40 km north.||Unit in Tumblagooda Sandstone.|||A distinctive, one metre thick pebbly sandstone to pebble conglomerate bed, useful as a stratigraphic marker.|
25917|Gabba Gabba Member|64635|6|Mentioned|p11, p12 Fig.10, p14  |Ordovician|Ordovician|A marker bed, extending c.40 km along the Murchison River. Marks the lowest appearance of vertical burrows such as Cylindricum or Skolithos.||Unit in Tumblagooda Sandstone.|||Distinctive pebbly sandstone to pebble conglomerate bed about 1 m thick.|
25917|Gabba Gabba Member|65313|5|Briefly described|p578, p584|Hirnantian|Hirnantian|Age based on paleomagnetic reverse to normal transition near the top of Tumblagooda Sandstone near this unit. May be glacial outwash.| ~442 Ma.|Of Tumblagooda Sandstone.|||Conglomerate.|26-MAR-12
80793|Gage Lowstand Fan|71958|2|Defined|p55-p59, p62, p64-p65, p67-p71|Valanginian|Valanginian|Vlaming Sub-basin. The name is derived from the Gage Sandstone with which it largely coincides. The type locality occurs in Warnbro 1 (-32.23769, 115.347327) in the interval between 2117.8 and 1949.5 m (total thickness of 164.3m). Age is derived from diagnostic microfossils particularly the lower G. mutabilis Dinocyst zone which contains the following microfossils: A. galeata, Batiacasphaera sp., P. charlottensis, A. saevus, L. bedfordii, P. horridus, A. dandangarensis, Ruffordia sp. and Australensis. Penetrated in eight petroleum exploration wells. It reaches a maximum thickness of 630m at the mouth of a large broad canyon adjacent to Mandurah Terrace/Badaminna Fault zone 20km northeasst of Warnbro1. Overlain by undifferentiated South Perth Sequence 2. Deposited in a sand-rich submarine fan system and includes deposits of turbidity currents, slumps, debrites and lateral accretionary packages. Abbreviated to Gage LSF on p68 and p69. See also p77, p80-p81, p84-p87, p104-p105, p107, p115, p148-p150, p157,  p162.||South Perth Sequence 2||Unconformably overlies the Jervoise Sandstone.|Poorly sorted, fine-grained to granular feldspathic sandstone interbedded with dark grey/black micaceous mudstone and siltstone.|
72709|Gairdner Dolerite|63224|5|Briefly described|p11||Neoproterozoic III|Formerly the Gairdner Dyke Swarm.  Geological Province: Gawler Craton.||||||07-FEB-08
72709|Gairdner Dolerite|64647|6|Mentioned|p46|||||||||
72709|Gairdner Dolerite|65221|5|Briefly described|p28 Fig.3a |Neoproterozoic|Neoproterozoic|||||||
72709|Gairdner Dolerite|65483|5|Briefly described|p19|Neoproterozoic|Neoproterozoic|Believed to be intrusive equivalent to Beda Volcanics. Age c. 825 Ma (Wingate et al 1998). Dykes of this unit intrude the northern part of the Cultana Subsuite.||||||28-JAN-11
72709|Gairdner Dolerite|65693|5|Briefly described|p4. |||Occurs in a series of dykes.|825 Ma.|||||
72709|Gairdner Dolerite|67375|4|Described|p54, p55, p262, p348.|Neoproterozoic|Neoproterozoic|Mostly NW- to N-trending; extend from the Gawler and Stuart Shelf to the Musgrave Province. Linked to Amata Dolerite (east Musgrave Province) on basis of similar chemistry and age. Metamorphosed during the Petermann Orogeny (c.570 to 550 Ma).|827 +/- 6 - 824 +/- 4 Ma (Glikson et al. 1996).|||Crosscuts the Warakurna Supersuite, Bentley Supergroup, Kullal Dyke Suite and norite of the Giles Suite.|Medium-grained, intergranular to subophitic dolerite; shows polygonal granoblastic texture where recrystallized.|
72709|Gairdner Dolerite|67553|5|Briefly described|p56,78-79|Tonian|Tonian|Geological province: Musgrave Province, North Australian Craton. Thickness: up to 150m at (BELL ROCK, MGA 481850E 7117850N). Crosscuts the c. 1000 Ma Kullal Dyke Suite and Giles layered intrusions.|c. 825 Ma||||Medium-grained, intergranular to subophitic dolerite.|
72709|Gairdner Dolerite|68067|6|Mentioned|Map legend.|||||||||27-AUG-13
72709|Gairdner Dolerite|68126|6|Mentioned|p29|Neoproterozoic|Neoproterozoic|||||||
72709|Gairdner Dolerite|68208|6|Mentioned|p32 Fig.3, p37|Neoproterozoic|Neoproterozoic|NW-trending anomalies in aeromagnetic data attributed to dykes of this unit.||||||
72709|Gairdner Dolerite|69003|5|Briefly described|p4, p59-60|Neoproterozoic|Neoproterozoic|West Musgrave Province, Paterson Orogen. Mantle plume activity associated with the break-up of Rodinia.|c.825 Ma.|||||
72709|Gairdner Dolerite|69019|5|Briefly described|p32-33, p78, p80-81 Figs.17,19, p142.|Neoproterozoic|Neoproterozoic|Forms a dyke swarm intruding the Gawler Craton. Described in comparison with Ooloo Hill Formation basalt.|827 +/- 6 Ma (baddeleyite: Wingate et al. 1998).|||||
72709|Gairdner Dolerite|69023|6|Mentioned|p55, p58|Neoproterozoic|Neoproterozoic|Forms a dyke swarm.||||||
72709|Gairdner Dolerite|69091|5|Briefly described|p77-78|||Extend from Gawler Craton and Stuart Shelf to Musgrave Province. c. 800 Ma event produced Gairdner Dolerite and Amata Dolerite.|c. 825 Ma|||Crosscuts Kullal Dyke Suite.||
72709|Gairdner Dolerite|69153|5|Briefly described|GEOCHRON/194759.1.pdf|Neoproterozoic|Neoproterozoic|Age mentioned in GEOCHRON/194759.1.csv file.|825 Ma, Glikson et al. 1996; Wingate et al. 1998|||cross-cuts Kullal Dyke Suite||24-MAR-16
72709|Gairdner Dolerite|69436|5|Briefly described|p21:15|||Howard et al. (2011). A dyke swarm which extends from the Gawler Range and Stuart Shelf in SA. Has similar age, geochemistry and eNd values to the Amata Dolerite.|||||Subophitic dykes with slightly enriched, primitive mantle-normalised, incompatible trace element geochemistry and eNd values of +2.39 and +3.81.|12-JUL-16
72709|Gairdner Dolerite|69648|5|Briefly described|p16|||Formerly Gairdner Dyke Swarm. Major swarm of dykes of variable magnetic character (dominated by positively magnetic dykes); generally trends NW-SE. Not recorded in any drilling on OOLDEA. Eastern Officer Basin.||||||17-FEB-15
72709|Gairdner Dolerite|69666|5|Briefly described|p24, p26-27, p33, p35-37|Neoproterozoic|Neoproterozoic|Part of the Willouran Basic Province. Intrudes central Gawler Craton. Inferred to be feeder dykes to the Beda Basalt and other volcanics of the Willouran Basic Province. Geochemistry described in some detail. Similar major and trace element abundances to Beda Basalt. Pb-Pb baddeleyite age.|827 +/- 7 Ma (Wingate et al., 1998).|||||
72709|Gairdner Dolerite|69729|5|Briefly described|p74 Fig.8, p84-86|Neoproterozoic|Neoproterozoic|Mostly NW-trending dykes extending from SE Gawler Craton to the west Musgrave Province. Trace element plot.|c.827-824 Ma.|||||
72709|Gairdner Dolerite|70333|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Other age determinations are Sm-Nd ages of 867 +/- 47 Ma and 802 +/- 35 Ma.|827 +/- 6 Ma (U-Pb).||||Dolerite dykes locally intruded by black basalt.|
72709|Gairdner Dolerite|70334|5|Briefly described|p2,10,14,42,44-47,76,83|Tonian|Tonian|Geological province: Gawler Craton. Dimensions: average 30km long, >50m wide (Flint et al., 1993). Consists of a swarm of NE-SW trending linear dolerite dykes, extends >1000 km in the Gawler Craton and Stuart Shelf (Parker et al., 1987, Preiss, 1987, Cowley and Flint, 1995), NW Musgrave Province (Zhao et al., 1994) and Broken Hill Domain (Hilyard, 1989, Crawford and Hilyard, 1990, Ernst et al., 2008). Age of intrusion constrained by SHRIMP U-Pb baddeleyite and zircon ages (827+\-6 Ma; Wingate et al., 1998), and Sn-Nd mineral isochrons (802+\-35 Ma and 867+\-47 Ma; Zhao et al., 1994).|827+\-6 Ma (U-Pb)|||Intrudes Moonabie and Pandurra formations, and Cultana Subsuite. Contemporaneous with Beda Basalt and Backy Point Formation; Littlle Broken Hill Gabbro.||14-OCT-19
72709|Gairdner Dolerite|70336|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|||||||
72709|Gairdner Dolerite|70339|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||Sm-Nd 867+/-47 and 802+/-35 Ma; U-Pb 827+/-6 Ma.||||Dolerite dykes locally intruded by black porphyritic basalt.|
72709|Gairdner Dolerite|70405|5|Briefly described|p79, p49|Neoproterozoic|Neoproterozoic||827 Ma ||||Mafic (metadolerite) dykes.|
72709|Gairdner Dolerite|70634|4|Described|100k_geologyp_lut,csv|Cryogenian|Cryogenian||824 Ma - 827 Ma||||Medium-grained dolerite and metadolerite; typically intergranular to subophitic; polygonal granoblastic where metamorphosed|
72709|Gairdner Dolerite|70658|6|Mentioned|p29|||||||||
72709|Gairdner Dolerite|70659|6|Mentioned|p10, p14, p375|Neoproterozoic|Neoproterozoic|Thin section description.||||||
72709|Gairdner Dolerite|70793|4|Described|GEOL_LUT_CSV files|Cryogenian|Cryogenian|Geological province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv.|827+\-6 Ma; 824+\-4 Ma|||Intrudes into Kullal Dyke Suite.|Medium-grained dolerite and metadolerite; typically intergranular to subophitic; polygonal granoblastic where metamorphosed|
72709|Gairdner Dolerite|70819|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|Clare Valley.|827 +/- 6 Ma (U-Pb).|||||
72709|Gairdner Dolerite|70826|6|Mentioned|p14 tbl 5|Tonian|Tonian|Musgrave and Rudall Provinces. Described as a dyke suite.|825 Ma|||||20-MAY-20
72709|Gairdner Dolerite|70839|5|Briefly described|p327,336,339|Tonian|Tonian|Geological province: Musgrave Province. NW-trending mafic dyke suite across northern South Australia into Musgrave region. Equivalent to Amata Dolerite.|827+\-6 Ma|||||
72709|Gairdner Dolerite|71037|5|Briefly described|p22-23 Fig.2, p27 Fig.6|Neoproterozoic|Neoproterozoic|SHRIMP U-Pb baddelyite age 827 +/- 6 Ma (Wingate et al., 1998). Shown as Willouran age [radiometric age equivalent to Tonian].|827 +/- 6 Ma.|||Shown as age equivalent to Backy Point Formation and younger than Pandurra Formation and older than Tapley Hill Formation.|Dolerite dykes.|
72709|Gairdner Dolerite|71129|4|Described|p1,15,17,35,103-106,184,207-208,225,227|Tonian|Tonian|Of Stuart Shelf. NW-trending dolerite dyke swarm; part of the Willouran Basic Province, which also includes the Wooltana, Cadlareena and Noranda volcanics, Wilangee Basalt and Little Broken Hill Gabbro, and Beda Basalt. Related to the Rodinian break-up (Zhao et al., 1994, Li et al., 1999, Wang et al., 2010). Basaltic volcanism interpreted to be result of mantle plume upwelling, causing doming in the continental lithosphere (Zhao et al., 1994). Contains tholeiitic, within-plate basaltic composition with commonly smooth LREE-enriched patterns and high initial ENd values; geochemically similar to high-Ti continental flood basalts. Geochemical analysis indicate derivation by large-scale decompression melting of a large heterogeneous asthenopheric mantle plume with no significant crustal contamination. Emplacement occurred immediately after Beda Basalt and Backy Point Formation deposition. Age contrained by SHRUMP U-Pb dating of zircons and baddelyite to 827+\-6 Ma (Wingate et al., 1998), supported by LA-ICPMS U-Pb of hydrothermal apatite and titanite from Olympic Dam samples, yielding ages of c. 820-825 Ma (Huang et al., 2016, Apukhtina et al., 2016).|827+\-6 Ma (SHRIMP U-Pb baddelyite)|||Equivalent to Amata Dolerite. Intrudes into Moonabie Formation or Wandearah Formation or Gluepot Granite or Broadview Schist or Gawler Range Volcanics.|Dolerite; porphyritic, variably contains plagioclase, clinopyroxene, titanomagnetite, lesser hornblende, biotite, small amounts of olivine. Commonly weathered to saprolite in outcrop.|
72709|Gairdner Dolerite|71130|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|SHRIMP U-Pb baddeleyite age.|827 +/- 6 Ma (Wingate et al., 1998).||||Dolerite dykes.|
72709|Gairdner Dolerite|71131|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|SHRIMP U-Pb baddeleyite age.|827 +/- 6 Ma (Wingate et al., 1998).||||Dolerite dykes.|
72709|Gairdner Dolerite|71169|6|Mentioned|p82|Tonian|Tonian||c. 825 Ma|||||
72709|Gairdner Dolerite|71235|6|Mentioned|p3-p5, p9|Neoproterozoic|Neoproterozoic|||||||
72709|Gairdner Dolerite|71236|6|Mentioned|p5, p28, p32|Tonian|Tonian|Believed to be the intrusive equivalent of the Beda Volcanics. Dykes which intrude the Cultana Subsuite are visible in magnetic imagery. |c. 827 +/- 6 Ma (Wingate et al., 1998)|||Intrudes the Cultana Subsuite.||16-MAR-23
72709|Gairdner Dolerite|71268|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Geological Province: Paterson Orogen. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv.|827+\-6 Ma; 824+\-4 Ma||||Medium-grained dolerite and metadolerite; typically intergranular to subophitic; polygonal granoblastic where metamorphosed|
72709|Gairdner Dolerite|71317|6|Mentioned|p15|Neoproterozoic|Neoproterozoic|Gawler Craton.||||||
72709|Gairdner Dolerite|71321|5|Briefly described|p1,11,50,64|Tonian|Tonian|Geological province: Musgrave Province. Intruded post-c. 1085-1040 Ma Giles Event (p11 for references).|c. 820 Ma|||Correlable to Amata Dolerite (Musgrave Province).||
72709|Gairdner Dolerite|71413|6|Mentioned|p32 Fig 2|||Geological province: Gawler Craton. ||||||
72709|Gairdner Dolerite|71416|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Geochronology by Wingate et al. (1998).|827 +/- 6 Ma (SHRIMP U-Pb baddeleyite age).|||Correlative of Amata Dolerite.||
72709|Gairdner Dolerite|71712|5|Briefly described|p411, p419|Tonian|Tonian|Age based on Pb\Pb badeleyite geochron.|827 +\- 6 Ma Pb-Pb baddelyite age|||Intrudes the Pandurra Formation.  Coeval with Beda Basalt.||31-MAR-20
72709|Gairdner Dolerite|71859|6|Mentioned|p18|Neoproterozoic|Neoproterozoic|||||||
72709|Gairdner Dolerite|71862|6|Mentioned|p8, p12|Neoproterozoic|Neoproterozoic|||||||
72709|Gairdner Dolerite|71895|4|Described|p10, p25, p61-p63, APP1. p19,-p20|Neoproterozoic|Neoproterozoic|Also intrudes crystalline basement. Recognised in geophysics as long, sub-parallel, linear magnetic anomalies. This unit is the intrusive equivalent of the Beda Basalt. Spectral analysis is provided. App5. p110, p162, p164, APP8. p202 .Petrogaphic descriptions for numerous samples are provided in App5.|c. 800 Ma|||Intrudes the Pandurra Formation.|Dolerite and basaltic rocks.|
72709|Gairdner Dolerite|72089|6|Mentioned|p11|||Gawler Craton. Intersected in MSDP04.||||||
72709|Gairdner Dolerite|72090|5|Briefly described|p42, p44, p46|||Gawler Craton.|||||Grey, massive, fine- to coarse grained dolerite.|
72709|Gairdner Dolerite|72237|6|Mentioned|p29|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton.||||||
72709|Gairdner Dolerite|72238|5|Briefly described|p34,42-44|Tonian|Tonian|Geological province: Musgrave Province. Part of the Gairdner LIP, alongside Amata Dolerite, Willouran Basic province and other coeval mafic igneous rocks (see p34 for references). SHRIMP U-Pb age of 827+\-6 Ma from baddeleyite and zircon extracted from a dolerite dyke sample from drillhole RL 1 (Reedy Lagoon, northwestern Stuart Shelf, SA Geodata drillhole number 16695; Wingate et al. 1998). LA-ICPMS U-Pb age of c. 825-820 Ma of magmatic apatite and hydrothermal apatite and titanite at Olympic Dam (Huang et al. 2015, Apukhtina et al. 2016). Related to the first magmatic cycle (c. 825-800 Ma) in the South China Block.||||Equivalent to Amata Dolerite.||
72709|Gairdner Dolerite|72242|6|Mentioned|p27,29|Tonian|Tonian|Geological province: Coompana Province, Western Gawler Craton.||||||
72709|Gairdner Dolerite|72344|6|Mentioned|p3|||Coompana Province.||||||
72709|Gairdner Dolerite|72725|6|Mentioned|p25-30|Tonian|Tonian|Dyke swarm with NNW-SSE trending dykes. Appear sparse and distributed in the 1A Tallaringa North survey area. Is preferentially expressed in many of the magnetic field enhancement images because the top of the dykes are shallower than most other strong magnetisations.|c. 820-830 Ma|||Intrudes Callana Group.||
72709|Gairdner Dolerite|73061|6|Mentioned|p1069|Neoproterozoic|Neoproterozoic|Gairdner Dyke Swarm in text. Gawler Craton.|~827 Ma|||||
72709|Gairdner Dolerite|73091|6|Mentioned|map legend||||||||Dolerite dykes.|30-NOV-21
72709|Gairdner Dolerite|73103|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Is also shown in the Solid Geology Interpretation map, below the main Whyalla 250k map. Sm-Nd ages of 867 +/- 47 Ma and 802 +/- 35 Ma are also given.|827 +/- 6 Ma (U-Pb).||||Dolerite dykes locally intruded by black porphyritic basalt.|
72709|Gairdner Dolerite|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Other age determinations given are 867 +/- 47 Ma (Sm-Nd), and 802 +/- 35 Ma (Sm-Nd).|827 +/- 6 Ma (U-Pb).||||Dolerite dykes locally intruded by black porphyritic basalt.|
72709|Gairdner Dolerite|73166|6|Mentioned|p644|Neoproterozoic|Neoproterozoic|Gawler Craton. Intrudes the Olympic Cu-Au Province.|0.83 Ga|||||
72709|Gairdner Dolerite|73188|6|Mentioned|p315|Tonian|Tonian|Geochron from Wingate et al. (1998). Accompanied earliest rifting in the Adelaide Geosyncline.|827 +/- 6 Ma|||||
72709|Gairdner Dolerite|73225|5|Briefly described|p5|||NW-trending dykes.|c.825 Ma.|||||
72709|Gairdner Dolerite|73227|6|Mentioned|p24|Tonian|Tonian|Geochron from Wingate et al. (1998). Interpreted as feeders for the Beda Basalt.|827 +/- 6 Ma|||Equivalent to Beda Basalt. Intrudes Pandurra Formation.||
72709|Gairdner Dolerite|73234|6|Mentioned|p6|Tonian|Tonian|Contemporaneous with Beda Basalt.|c. 825 Ma|||||
72709|Gairdner Dolerite|73235|6|Mentioned|p53|Tonian|Tonian||c. 825 Ma|||||
72709|Gairdner Dolerite|74361|6|Mentioned|p164, 177|Neoproterozoic|Neoproterozoic|Intrudes the northern and eastern Gawler Craton.|c.830 Ma.||||Mafic dykes.|
72709|Gairdner Dolerite|74367|5|Briefly described|p8, p18|Tonian|Tonian|Suggested to be coeval with Noranda Volcanics, Cadlareena Volcanics, Beda Basalt, Willangee Basalt and the 'Depot Creek Volcanics'. Correlation with Boucaut Volcanics has proven to be incorrect.|827+/-6 Ma|||Correlated with Wooltana Volcanics||
28112|Galawa Member|13194|4|Described|p395 Tb. 4-16, p399 fig 4-63|||Type Section: Hart Spring 15o26'S 128o39'E. 5-47m thick partially exposed carbonate-sand bank.||Skewthorpe Formation||Overlies Mulali Member (conformably). Overlain by Djigumirri Member (conformably).|Oolitic sandy dolomite; rare sandstone and shale.|
28112|Galawa Member|40993|2|Defined|p2|Cambrian|Cambrian|||||||
28112|Galawa Member|41864|4|Described|p38|||||||||
32535|Galeru Member|66127|3|Fully described|pp127-132, pp163-165, p286, Plates 4,5,7|Late Frasnian|Late Frasnian|Of Hocking and Playford (1998d). Named after Galeru Gorge. Type section is NW of Lawford Spring. c.1900 m thick. Age also shown as Givetian to Famennian. Poorly exposed. Deposition cycles discussed in detail.||Unit in Sparke Conglomerate.|||Distinctive cyclic sequence, each averaging 11-12m thick, coarsening upwards, commonly from marine siltstone or sandstone at the base to subaerial boulder conglomerate at the top.|
23605|Galloping Creek Formation|13194|4|Described|p393 Tb. 4-16, p402 fig 4-66|Frasnian|Frasnian|Type Section: 10.5km south "Glenhill", 16o23'S 128o36'E. 1600-2000m thick alluvial fan and fluvial deposits.  Only found in Ragged Range outlier and Mount Brooking.||||Overlies Antrim Plateau Volcanics and Kellys Knob Sandstone (both unconformably). Laterally equivalent to Abney Sandstone and Ragged Range Conglomerate.|Pebbly feldspathic sandstone, conglomerate; minor siltstone.|
23605|Galloping Creek Formation|22547|4|Described|p30||Late Devonian|Of the Cockatoo Group. Geological province: Bonaparte Basin. Thickness: 1600 m.||||||14-NOV-06
23605|Galloping Creek Formation|40993|2|Defined|p5|Frasnian|Frasnian|||||||
23605|Galloping Creek Formation|41864|3|Fully described|p52|||Previously mapped as Ragged Range Conglomerate.||||||15-DEC-08
23605|Galloping Creek Formation|41865|5|Briefly described|Map legend|Frasnian||||||||
23605|Galloping Creek Formation|42030|5|Briefly described|p749|||||||||
23605|Galloping Creek Formation|43853|5|Briefly described|Map Legend||Frasnian|||||||
23605|Galloping Creek Formation|44230|5|Briefly described|Map Legend||Frasnian|||||||
23605|Galloping Creek Formation|64580|6|Mentioned|map legend|||Of Cockatoo Group.||||||15-DEC-08
23605|Galloping Creek Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Frasnian|Frasnian|Southern Bonaparte Basin||Cockatoo Group|||Pebbly feldspathic sandstone and conglomerate; minor siltstone.|31-JUL-15
23605|Galloping Creek Formation|69165|5|Briefly described|100k_interpgeop_lut.csv|Frasnian|Frasnian|See also 500k_geologyp08_lut.csv. ||Cockatoo Group|||Pebbly feldspathic sandstone and conglomerate; minor siltstone.|
23605|Galloping Creek Formation|69452|6|Mentioned|p36:6|Frasnian|Frasnian|||Cockatoo Group.||||12-JUL-16
23605|Galloping Creek Formation|69634|4|Described|100k_interpgeop_lut.csv|Frasnian|Frasnian|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny; Mount Eclipse Movement; Pertnjara-Brewer Movements.|382.7-372.2 Ma (Inferred)|Unit of Cockatoo Group.|||Pebbly feldspathic sandstone and conglomerate; minor siltstone|
23605|Galloping Creek Formation|70154|4|Described|100k_interpgeop_lut.csv|Frasnian|Frasnian|||Cockatoo Group|||Pebbly feldspathic sandstone and conglomerate; minor siltstone.|
23605|Galloping Creek Formation|70812|6|Mentioned|p30|||||||||
23605|Galloping Creek Formation|71267|5|Briefly described|100k_interpgeop_lut.csv|Frasnian|Frasnian|Geological Province: Halls Creek Orogen. Of Southern Bonaparte Basin. Events: Alice Springs Orogeny (450-295 Ma); Eclipse Movement (340-300 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma).|382.7-372.2 Ma (inferred)|Unit of Cockatoo Group.|||Pebbly feldspathic sandstone and conglomerate; minor siltstone|
34801|Galtee Moore|22774|5|Briefly described|p573|||Age of unit 2810+/-19 Ma||||||
29419|Gamma Island Formation|42959|4|Described|p63|||See also Fig.3 p58||||||
29419|Gamma Island Formation|65194|5|Briefly described|p136 Fig.4.37|Miocene|Oligocene|Dolomite and dolomitic carbonate mudstone. Shown as lenses within Revenge Formation.||||||11-APR-16
26566|Gamminah Conglomerate|30388|4|Described|Table 1|||Middle Proterozoic age. On P11||||||
26566|Gamminah Conglomerate|30390|4|Described|p77|||||||||
26566|Gamminah Conglomerate|30944|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|of the Mission Group||||||25-NOV-08
26566|Gamminah Conglomerate|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
26566|Gamminah Conglomerate|36551|6|Mentioned|Table 31|||||||||
26566|Gamminah Conglomerate|36886|4|Described|p198|||||||||
26566|Gamminah Conglomerate|67375|5|Briefly described|p38 Table 1, pp50-51. |Mesoproterozoic|Mesoproterozoic|Locally restricted. Grades upwards into the sandstone-shale succession of the lower Frank Scott Formation.||Basal unit in Frank Scott Formation.||Overlies Miller Basalt of the Cassidy Group. Is overlain by Frank Scott Formation.|Moderately coarse-grained; sub-rounded to well-rounded pebbles and cobbles; clasts of amygdaloidal basalt, felsic porphyritic volcanic rock, and milky quartz; intercalated thin sandstone layers with parallel lamination.|
26566|Gamminah Conglomerate|67553|4|Described|p40,53|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Talbot Sub-basin, Bentley Sub-basin. A locally restricted basal member of the Frank Scott Formation.||Unit of Frank Scott Formation.||Lowermost unit of Mission Group. Overlain by Frank Scott Formation. Underlain by Miller Basalt/Cassidy Group.|Moderately coarse-grained, subrounded to well-rounded pebbles and cobbles up to about 20 cm in diameter. These clasts are mainly composed of amygdaloidal basalt, felsic porphyritic volcanic rock, and milky quartz.|
26566|Gamminah Conglomerate|68995|5|Briefly described|p10, p19|Stenian|Stenian|Contains crude planar bedding, ripple cross lamination and some cross bedding within the sandstones. Also minor trough cross bedding typical of fluvial depositional environments.||Mission Group||Overlies the Miller Basalt. Overlain by the Frank Scott Formation.|Moderately coarse-grained rock containing subrounded to well-rounded pebbles and cobbles up to about 20cm in diameter.  The conglomerate is intercalated with thin sandstone layers.|
26566|Gamminah Conglomerate|69091|5|Briefly described|p75|||||Mission Group|||Sedimentary.|26-SEP-14
26566|Gamminah Conglomerate|69153|5|Briefly described|GEOL_LUT_CSV files; Rocks.csv|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen. Sample descriptions include: conglomerate, sandstone||Mission Group|||Matrix-supported pebble to cobble conglomerate; basalt and rhyolite clasts up to 20 cm; thin sandstone interlayers|
26566|Gamminah Conglomerate|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Mission Group.||Is overlain by Frank Scott Formation.|Matrix-supported pebble to cobble conglomerate; basalt and rhyolite clasts up to 20cm; local planar- and cross-bedding; thin sandstone interlayers.|
26566|Gamminah Conglomerate|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic||1040 Ma - 1057 Ma (Inferred)|Mission Group|||Matrix-supported pebble to cobble conglomerate; basalt and rhyolite clasts up to 20 cm; local planar- and cross-bedding; thin sandstone interlayers|
26566|Gamminah Conglomerate|70793|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv.|1057-1040 Ma (inferred)|Unit of Mission Group.|||Matrix-supported pebble to cobble conglomerate; basalt and rhyolite clasts up to 20 cm; local planar- and cross-bedding; thin sandstone interlayers|
26566|Gamminah Conglomerate|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone|
26566|Gamminah Conglomerate|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 1m_geologyp12_lut.csv.|1057-1040 Ma (inferred)|Unit of Mission Group.|||Matrix-supported pebble to cobble conglomerate; basalt and rhyolite clasts up to 20 cm; local planar- and cross-bedding; thin sandstone interlayers|
24996|Gap Creek Formation|7433|6|Mentioned|p25 Fig.2. |||Canning Basin.||||||
24996|Gap Creek Formation|13995|5|Briefly described|p73, p77, p82, p99|Ordovician|Ordovician|Canning Basin, WA. Brachiopod, gastropod, trilobite species listed. Late Bendigonian age.||||Overlies Emanuel Formation.||
24996|Gap Creek Formation|14228|5|Briefly described|p6 fig3|Arenig|Arenig|North Canning Basin.||||Overlies Emanuel Formation. Overlain by Willara Formation.||05-OCT-16
24996|Gap Creek Formation|22646|6|Mentioned|Fig 5 on p 105|Early Ordovician|Early Ordovician|Canning Basin.  Age - Arenig.||||||
24996|Gap Creek Formation|22741|5|Briefly described|P21, Table3 P18||Early Ordovician|||||||
24996|Gap Creek Formation|22764|6|Mentioned|p13||Early Ordovician|Prices Creek Group.||||||01-FEB-10
24996|Gap Creek Formation|22767|6|Mentioned|P11|||Correlates with the Willara Formation||||||
24996|Gap Creek Formation|23373|6|Mentioned|p318||Early Ordovician|Of Canning Basin.||||||10-NOV-08
24996|Gap Creek Formation|23847|5|Briefly described|p297 Fig. 1|Ordovician|Ordovician|Geological Province: Canning Basin.||||||
24996|Gap Creek Formation|24061|6|Mentioned|p177|||Geological Province: Canning Basin.||||||10-NOV-08
24996|Gap Creek Formation|29813|6|Mentioned|p16|||||||||
24996|Gap Creek Formation|30110|6|Mentioned|p81|||Llanvirnian age.||||||
24996|Gap Creek Formation|30983|4|Described|p74|||||||||
24996|Gap Creek Formation|31332|6|Mentioned|Fig. 3|||||||||
24996|Gap Creek Formation|31706|6|Mentioned|p637|||Ordovician correlation chart||||||
24996|Gap Creek Formation|32648|6|Mentioned|p32|||Ordovician||||||
24996|Gap Creek Formation|33042|6|Mentioned|Fig.1|||See also Fig.4 Ord.||||||
24996|Gap Creek Formation|33518|6|Mentioned|p4|||||||||
24996|Gap Creek Formation|34999|6|Mentioned|p124|||||||||
24996|Gap Creek Formation|35119|4|Described|p461|||Mention Text-Fig.3.||||||
24996|Gap Creek Formation|36122|6|Mentioned|p11|||||||||
24996|Gap Creek Formation|36225|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
24996|Gap Creek Formation|36257|6|Mentioned|Table 2.1|||||||||
24996|Gap Creek Formation|36890|3|Fully described|p322|||Formerly Gap Creek Dolomite.||||||10-NOV-08
24996|Gap Creek Formation|38878|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
24996|Gap Creek Formation|40136|5|Briefly described|p25|||||||||
24996|Gap Creek Formation|41055|6|Mentioned|p46|||||||||
24996|Gap Creek Formation|41169|6|Mentioned|Fig.3|||||||||
24996|Gap Creek Formation|41215|6|Mentioned|p265|||||||||
24996|Gap Creek Formation|41730|6|Mentioned|p472|||||||||
24996|Gap Creek Formation|41854|6|Mentioned|p94|||||||||
24996|Gap Creek Formation|42080|5|Briefly described|Fig.2 P281|||||||||
24996|Gap Creek Formation|42347|6|Mentioned|Fig.2 P1020|||||||||
24996|Gap Creek Formation|42880|5|Briefly described|Fig.2,p1020|||||||||
24996|Gap Creek Formation|42994|5|Briefly described|p104|||||||||
24996|Gap Creek Formation|43656|6|Mentioned|Fig.2,p8|Arenigian|Arenigian|||||||
24996|Gap Creek Formation|43666|6|Mentioned|p20,49 Table 2||Early Ordovician|||||||
24996|Gap Creek Formation|43803|3|Fully described|p65,68|||||||||
24996|Gap Creek Formation|43808|5|Briefly described|p298|||||||||
24996|Gap Creek Formation|43809|6|Mentioned|Fig.3,p215|||||||||
24996|Gap Creek Formation|44143|4|Described|p.441 Table 4-19|Ordovician|Ordovician|Unit in Prices Creek Group. Up to 192m thick; dolomite, siltstone & sandstone; shallow marine. Conformably overlies Emanuel Formation. Type section near Gap Creek (NOONKANBAH: 18deg 35' S; 125 deg 55' E). Contains brachiopods, conodonts: late Arenigian to earliest Llanvirnian.||||||
24996|Gap Creek Formation|44403|2|Defined|p.8|||E/51-12, dolomite, silty dolomitic limestone, sandy bands common, marine fossils. O/lain unconformably by Pillara Formation. U/lain conformably by Emanuel Formation.||||||
24996|Gap Creek Formation|44404|14|Not recorded|map legend||Ordovician|||||||
24996|Gap Creek Formation|44998|2|Defined|p20|||Fig 4. On many pages. p.18,221,223.||||||
24996|Gap Creek Formation|45101|6|Mentioned|Fig.8|||||||||
24996|Gap Creek Formation|45153|2|Defined|App.1-15|Middle Ordovician|Middle Ordovician|Previously named Gap Creek Dolomite.||||||
24996|Gap Creek Formation|45158|3|Fully described|p28|||||||||
24996|Gap Creek Formation|50089|5|Briefly described|p427, p430 Fig. 5|Ordovician|Ordovician|Oepikodus communis (conodont) found.  Overlies Emanuel  Formation. Geological Province: Canning Basin.||||||
24996|Gap Creek Formation|62794|5|Briefly described|p298|Early Ordovician|Early Ordovician|Canning Basin. Overlies Emanuel Formation. Probably coeval with Horn Valley Siltstone in the Amadeus Basin, based on conodont (Oepikodus communis) and trilobite (Carolinites ?genacinaca) faunas.||||||05-DEC-12
24996|Gap Creek Formation|63938|5|Briefly described|p48, 51|Ordovician|Ordovician|Of Prices Creek Group. Overlain by Cadjebut Formation in Gap Creek-1, Prices Creek area.||||||
24996|Gap Creek Formation|64334|5|Briefly described|p38 Fig.2, p39-41, 43-46|Ordovician|Ordovician|Eastern Lennard Shelf, Canning Basin. Arenig. Detrital zircon analyses and plots; ages and provenances discussed.||Prices Creek Group.||Overlies Emanuel Formation.|Dolostone.|
24996|Gap Creek Formation|64580|6|Mentioned|map legend|||Of Prices Creek Group.||||||15-DEC-08
24996|Gap Creek Formation|64643|4|Described|p6, p5 Fig. 4, p22, p25 fig.21, p33, 36|Ordovician|Ordovician|Of Prices Creek Group. Dolomitic sandstone and siltstone. Type section in Emanuel Range. 223m thick. Mudstone and nodular carbonate, fine-grained brown dolomite with poor exposure above.||||||
24996|Gap Creek Formation|66127|5|Briefly described|p24, p26, Plates 4, 5, 7.|Middle Ordovician|Early Ordovician|||Unit in Prices Creek Group.  ||Is overlain unconformably by Cadjebut Formation.|Shallow-marine dolomitic sandstone and siltstone.|
24996|Gap Creek Formation|69099|5|Briefly described|500k_geologyp08_lut.csv|Middle Ordovician|Early Ordovician|||Prices Creek Group||||
24996|Gap Creek Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Ordovician|Ordovician|||Prices Creek Group||||
24996|Gap Creek Formation|69883|5|Briefly described|p4-p5|Arenig|Arenig|Canning Basin. Conodont zones and supersequences provided.||Prices Creek Group||Overlies the Emanuel Formation.|Carbonate and mudstone.|
24996|Gap Creek Formation|71171|6|Mentioned|p2|||Canning Basin.||||||
24996|Gap Creek Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Prices Creek Group.|||Shallow marine dolomite and silty dolomitic limestone with sandy interbeds|
24996|Gap Creek Formation|72497|5|Briefly described|p3 Fig.2.|Early Ordovician|Early Ordovician|Shown as occuring as part of the Lennard Shelf and Margaret Terrace.||||Conformably overlies Emanuel Formation.||
24996|Gap Creek Formation|73344|5|Briefly described|p3-4, p6, p41, p51, p56|Dapingian|Floian|Canning Basin, Lennard Shelf. Defined by Guppy and Opik (1950); amended by Guppy et al. (1958). Type section from 192 m of outcrop near Gap Creek. Part of supersequence A1. Includes the first appearance of O. communis and the coinciding eponymous biozone, and the J. gananda biozone.||Prices Creek Group||Underlain by Emanuel Formation. Equivalent to Willara Formation and Nambeet Formation including Samphire Marsh Member.||07-DEC-22
24996|Gap Creek Formation|73567|6|Mentioned|p62, p68-69|Ordovician|Ordovician|Canning Basin, Lennard Shelf.||Prices Creek Group||Equivalent to the Nambeet and Willara formations.||
32781|Gap Intrusion|44229|5|Briefly described|Map Legend|Archean|Archean|Intrudes the Pilbara Supergroup.||||||18-NOV-08
32781|Gap Intrusion|60429|2|Defined|p13,  p36 Appdx. 1|Archean|Archean|Large, concordant, mafic body within Apex Basalt - layered with serpentinized dunite cumulate at base + metapyroxenite at top; bulk of the body is serpentinized peridotite. Intruded by Coppin Gap Granodiorite. Age: c.3471-3314Ma. Max. thickness: ~1000m.||||Intruded by Coppin Gap Granodiorite. Post-dates Duffer Formation (3471+/-5 Ma)||27-JAN-17
32781|Gap Intrusion|64936|5|Briefly described|map legend|Archean|Archean|Serpentinized metadunite and serpentinite schist; metapyroxenite. Shown associated with Kelly Subgroup units. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
32781|Gap Intrusion|66217|5|Briefly described|p33|Paleoarchean|Paleoarchean|Maximum thickness: 500m. May be related to/contemporaneous with Strutton Intrusion. Interpreted to represent subvolcanic intrusions to the Euro Basalt.|||||Thick sill of serpentinized peridotite, dunite, and pyroxenite.|
32781|Gap Intrusion|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Emu Pool Supersuite.|||Serpentinized dunite and serpentine schist; minor metapyroxenite.|06-JAN-15
32781|Gap Intrusion|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Warrawoona Group|||Serpentinized peridotite, serpentinite, dunite, and pyroxenite; metamorphosed.|
32781|Gap Intrusion|69185|5|Briefly described|GEOL_LUT_CSV files||Archean|Geological province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_interpgeop_pilcrat02_lut.csv, 500k_interpgeol_pilcrat02_lut.csv.||||||
32781|Gap Intrusion|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||serpentinite, pyroxenite, ultramafic schist|
32781|Gap Intrusion|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Warrawoona  Large Igneous Province.||Warrawoona Group|||Serpentinized peridotite, dunite, and pyroxenite.|
23608|Gap Well Formation|23724|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Bangemall Group.||||||08-SEP-08
23608|Gap Well Formation|23725|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Bangemall Group.||||||
23608|Gap Well Formation|24183|6|Mentioned|p10|||||||||
23608|Gap Well Formation|41144|3|Fully described|p808|||||||||
23608|Gap Well Formation|50226|6|Mentioned|p428|||Hosts a polymetallic deposit in dolomitic siltstone and shale.||||||
23608|Gap Well Formation|64287|5|Briefly described|p33, p34 Fig. 2|||Of Bangemall Supergroup. Includes Woodlands Arenite (Member?). Includes dolomitic siltstone and shale hosting Abra base metal deposit. Disconformably overlain West Creek Formation. Details of ore minerals+lithology given.Geol.prov: Jillawarra Sub-basin||||||07-FEB-11
23608|Gap Well Formation|66241|5|Briefly described|p1, p2, p7, p11. |||Correlates with the Irregully Formation. The upper part of this unit, with the lower part of the overlying West Creek Formation, hosts the major Abra Pb-Ag-Cu-Au deposit.||||Is overlain by West Creek Formation.||
39606|Garden Creek Monzogranite|24531|5|Briefly described|p29, p8-9 Fig. 3|Archean|Archean|Of the Shaw Granitoid Complex. Medium-grained, leucocratic, biotite monzogranite, affected by very strong tectonic foliation. Intruded by the Coondina Monzogranite.||||||15-APR-13
39606|Garden Creek Monzogranite|24532|5|Briefly described|Map legend|Archean|Archean|Of the Shaw Granitoid Complex.||||||07-NOV-08
39606|Garden Creek Monzogranite|50427|5|Briefly described|p187 Fig.8|Archean|Archean|Of Shaw Granitoid Complex.||||||07-NOV-08
39606|Garden Creek Monzogranite|63441|5|Briefly described|p13 tb. 2|Archean|Archean|Geological Province: Pilbara Craton.||||||15-APR-13
39606|Garden Creek Monzogranite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Cleland Supersuite. Meta biotite monzogranite; tectonically foliated; leucocratic; minor pegmatitic granitic sheets.||||||
39606|Garden Creek Monzogranite|68282|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Cleland Supersuite|||Meta biotite monzogranite, tectonically foliated, leucocratic, minor pegmatitic granitic sheets; meta muscovite-biotite leucogranite, heterogeneous, medium- to coarse-grained, some tourmaline pegmatite veins.|03-DEC-14
39606|Garden Creek Monzogranite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Cleland Supersuite|||Meta biotite monzogranite; tectonically foliated; leucocratic; minor pegmatitic granitic sheets. Meta muscovite-biotite leucogranite; heterogeneous, medium to coarse grained; local patches with garnet or k-feldspar phenocrysts.|
39606|Garden Creek Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|3274-3224 Ma (inferred)|Unit of Cleland Supersuite.|||Metamorphosed muscovite-biotite monzogranite; tectonically foliated; leucocratic; minor pegmatitic granitic sheets|
39606|Garden Creek Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, granite|
39606|Garden Creek Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|||Cleland Supersuite|||Metamorphosed biotite monzogranite; tectonically foliated; leucocratic; minor pegmatitic granitic sheets.|
74870|Garden Rock Monzogranite|64891|5|Briefly described|p37 Fig. 2, p52-53 Tb. 1|Archean|Archean|Of Walganna Suite (Bald Rock Supersuite). Age: c. 2625Ma. Geological province: Murchison Domain. Monzogranite to syenogranite; post-tectonic.||||||07-FEB-11
74870|Garden Rock Monzogranite|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c.2617 Ma.|Unit in Walganna Suite.|||Monzogranite to syenogranite; undeformed.|
74870|Garden Rock Monzogranite|67129|6|Mentioned|p19 fig 20|Archean|Archean|Murchison Domain, Youanmi Terrane.||Bald Rock Supersuite|||Monzogranite.|07-SEP-17
74870|Garden Rock Monzogranite|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane.||Walganna Suite|||Monzogranite to syenogranite; K-feldspar porphyritic monzogranite; common magmatic foliation; undeformed.|05-NOV-15
74870|Garden Rock Monzogranite|69014|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Murchison Domain.||Of the Walganna Suite.|||Monzogranite to syenogranite; undeformed.|01-MAY-14
74870|Garden Rock Monzogranite|69583|5|Briefly described|p42-43, p49, p52, p113-114, p117-118|Neoarchean|Neoarchean|See also p121; Plate 2. Murchison Domain. Truncates the Cundimurra Shear Zone. About 20 x 30 km pluton.|2617 +/- 24 Ma (Wang, 1998).|Walganna Suite.|||Undeformed monzogranite with aligned euhedral feldpar (and locally hornblende) phenocrysts, mafic enclaves and schlieren layering.|
74870|Garden Rock Monzogranite|69584|5|Briefly described|p5 Fig.2|Neoarchean|Neoarchean|||Walganna Suite|||Monzogranite.|
74870|Garden Rock Monzogranite|69586|5|Briefly described|p6, p22-23, p25|Neoarchean|Neoarchean|Post-kinematic pluton. A medium-sized, slightly E-W elongate, undeformed pluton (~20 x 10 km). Appears as Garden Rock Granite on p6.|2617 +/- 24 Ma (Wang, 1998).|Walganna Suite.|||Contains euhedral K-feldspar phenocrysts.|
74870|Garden Rock Monzogranite|69627|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton|c. 2617 Ma|Walganna Suite|||Monzogranite to syenogranite; undeformed.|
74870|Garden Rock Monzogranite|69744|6|Mentioned|p254-255|||Murchison Domain, Youanmi Terrane. Post-tectonic; has a well-developed magmatic fabric discordant to regional structures.|2627 Ma.|||||
74870|Garden Rock Monzogranite|70139|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton. The two facies are mapped separately.|c.2617 Ma (Wang, 1998 unpub.).|Walganna Suite.|||Undeformed monzogranite to syenogranite; undeformed K-feldspar porphyritic monzogranite, common magmatic foliation.|
74870|Garden Rock Monzogranite|70796|5|Briefly described|100k_interpgeop_lut.csv|Mesoarchean|Mesoarchean|Yilgarn Craton. See also 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, Austin100_2442_stratig.pdf, Reedy100_2543_stratig.pdf, Wynyangoo100_2542_stratig.pdf.||Walganna Suite|||Monzogranite to syenogranite; undeformed. Kfeldspar porphyritic monzogranite; undeformed with a common magnetic foliation.|
74870|Garden Rock Monzogranite|70830|6|Mentioned|p8|||Murchison Domain. ||||||
74870|Garden Rock Monzogranite|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeol_lut.csv.|2650-2600 Ma (inferred)|Unit of Walganna Suite.|||Monzogranite to syenogranite; undeformed; K-feldspar porphyritic monzogranite; undeformed; common magmatic foliation.|
74870|Garden Rock Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|||Walganna Suite|Includes one unnamed subunit.||Monzogranite to syenogranite; undeformed.K-feldspar porphyritic monzogranite; undeformed; common magmatic foliation.|
74870|Garden Rock Monzogranite|73410|5|Briefly described|p4, 7, 11|||Youanmi Terrane. Truncates structures along the c.2660 Ma Cundimurra shear zone.|2624 +/- 3 Ma (Lu et al., 2018).||||Synorogenic granitic pluton. Undeformed.|
25918|Garford Formation|22587|6|Mentioned|p79 Fig.7|Middle Miocene|Early Miocene|||||||
25918|Garford Formation|22613|4|Described|p23|Miocene|Miocene|||||||
25918|Garford Formation|22614|5|Briefly described|map|Pliocene|Miocene|||||||
25918|Garford Formation|22916|5|Briefly described|12|||||||||
25918|Garford Formation|22938|6|Mentioned|p236|||||||||
25918|Garford Formation|23343|5|Briefly described|39|Miocene|Miocene|||||||
25918|Garford Formation|23479|5|Briefly described|p26|Neogene|Neogene|In palaeochannels incised into Eromanga Basin sediments||||||04-NOV-10
25918|Garford Formation|24358|5|Briefly described|p32|Early Pliocene|Late Miocene|Geological Province: Eucla Basin.||||||17-MAR-05
25918|Garford Formation|24396|4|Described|p216, p218 Fig.3|Early Pliocene|Middle Miocene|Lacustrine calcareous clays/carbonates. Contains the Kingoonya Member. See also p220 Fig.4, p222 Fig.5. Overlying the Gawler Craton.||||||04-NOV-10
25918|Garford Formation|24606|5|Briefly described|p956, p958 Fig. 3|Early Pliocene|Middle Miocene|Overlain by the Narlaby Formation. Geological Province: Eucla Basin.||||||
25918|Garford Formation|35080|2|Defined|p8|middle Tertiary|middle Tertiary|||||||
25918|Garford Formation|36244|6|Mentioned|p2|||Refers Benbow & Pitt 1978 for a definition.||||||
25918|Garford Formation|36966|6|Mentioned|p86|||||||||
25918|Garford Formation|37852|6|Mentioned|Fig.3|||||||||
25918|Garford Formation|38604|6|Mentioned|Map legend|Miocene|Miocene|||||||
25918|Garford Formation|38605|4|Described|p29|||See also Table 5.||||||
25918|Garford Formation|40912|6|Mentioned|Map legend|Pliocene|Miocene|Miocene-Pliocene||||||
25918|Garford Formation|41619|6|Mentioned|Map legend|Tertiary||||||||
25918|Garford Formation|42356|4|Described|Microfiche 7pp18|Miocene||See also DESC p18, Fig15 P119 Microfiche 7 p15, Fig.4, Fig.9, 10, 12, 13.||||||16-APR-18
25918|Garford Formation|42465|5|Briefly described|Map Legend|||||||||
25918|Garford Formation|42466|5|Briefly described|Map Legend|||||||||
25918|Garford Formation|42469|5|Briefly described|p39, p46|||||||||
25918|Garford Formation|42475|3|Fully described|p21|||||||||
25918|Garford Formation|42546|5|Briefly described|Map legend|Tertiary||||||||
25918|Garford Formation|42736|5|Briefly described|map legend|Tertiary||||||||
25918|Garford Formation|42816|3|Fully described|p24|||||||||
25918|Garford Formation|43053|5|Briefly described|Map Legend|Pliocene|Miocene|Lacustrine dolomite, clay, sand and silt. Geological Province: Eucla Basin palaeodrainage.||||||25-MAY-05
25918|Garford Formation|43258|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
25918|Garford Formation|43298|6|Mentioned|Map Legend|Pliocene|Miocene|||||||
25918|Garford Formation|43686|6|Mentioned|p236|||||||||
25918|Garford Formation|44133|5|Briefly described|p185, 180 Fig. 10.22|Pliocene|Pliocene|Geological Province: Eucla Basin. Thickness: 20m. Underlies: Narlaby Formation.||||||
25918|Garford Formation|44695|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
25918|Garford Formation|44935|5|Briefly described|Map Legend||Pliocene|||||||
25918|Garford Formation|60497|5|Briefly described|p42|Early Pliocene|Middle Miocene|Includes the Kingoonya Member.  Geological Province: Eucla Basin.||||||
25918|Garford Formation|60953|5|Briefly described|Map Legend|Pliocene|Miocene|Lacustrine dolomite, clay, sand and silt. Geological Province: Eucla Basin. Paleodrainage.||||||27-APR-05
25918|Garford Formation|61108|5|Briefly described|map legend|Pliocene|Miocene|Lacustrine dolomite, clay, sand and silt. Geological Province: Eucla Basin palaeodrainage.||||||
25918|Garford Formation|61155|5|Briefly described|p17|Early Pliocene|Early Miocene|Age: 18.5-14.5Ma; and, 5.5-4.0Ma. Max. thickness for older section: 70m. Geological Province: Eucla Basin; also in the Oodnadatta area||||||
25918|Garford Formation|61234|4|Described|p6, p7 Fig 4.|Early Pliocene|Middle Miocene|Geological Province: Eucla Basin. Overlies Khasta Formation unconformably. Lacustrine mudstone and dolomitic limestone.||||||14-MAY-07
25918|Garford Formation|61814|5|Briefly described|p26|Miocene|Miocene|Predominantly lacustrine clays. Geological Province: Gawler Craton.||||||08-FEB-10
25918|Garford Formation|61839|5|Briefly described|p227|Miocene|Eocene|Predominantly lacustrine clays. Overlying Gawler Craton.||||||04-NOV-10
25918|Garford Formation|64646|6|Mentioned|p23 Fig. 3, p24 Fig. 4|Pliocene|Middle Miocene|Includes Kingoonya Member. In palaeovalleys overlying Gawler Craton.||||||04-NOV-10
25918|Garford Formation|65194|5|Briefly described|p163-164, p171-172|Early Pliocene|Middle Miocene|Tallaringa and Garford palaeovalleys. Includes Kingoonya Member. Predominantly alkaline lacustrine and flood-plain deposits: very fine to coarse sand and silt, grading upwards into clay, dolomitic clay and dolomite. Associated with uranium mineralisation. Overlies Pidinga Formation unconformably.||||||11-APR-16
25918|Garford Formation|65385|4|Described|pS127, pS129 Fig.3|Late Eocene|Late Eocene|Unconformably overlies Pidinga Formation. Unconformably overlain by chalcedonic limestone. Consists of dolomitic clays, clayey sands and dolomitic limestones. Marginal marine to estuarine facies sediments representing a marine transgression.||||||08-MAR-12
25918|Garford Formation|65922|5|Briefly described|p25 Tb. 4, p26|Pliocene|Miocene|Khaki to greenish grey to brown, well-laminated to locally flaggy clay, silt and sand. Derived from Hutchison Group and locally, Gawler Range Volcanics and Hiltaba Suite. Overlies either Pidinga Formation or weathered basement. ||||||
25918|Garford Formation|67462|5|Briefly described|Map legend.|Neogene|Neogene|Eucla Basin; Gawler Craton. Shown as two seperate intervals, one middle Miocene, the other Late Miocene to Piocene.|||Includes Kingoonya Member.|||05-DEC-13
25918|Garford Formation|67921|5|Briefly described|Map legend|Pliocene|Miocene|||||Equivalent to Mangatitja Formation.|Lacustrine deposits of chalcedonic limestone and grey, green or red clayey sand to sandy clay.|
25918|Garford Formation|68128|5|Briefly described|p27, p43, p64, p71, p77|Pliocene|Eocene|Gawler Craton. Deposited in a lacustrine environment.|||||Mudstone, carbonate, minor sandstone.|31-JAN-23
25918|Garford Formation|68715|6|Mentioned|p30 Fig.5|Zanclean|Burdigalian|SW and NW Gawler Craton, Eucla Basin.||||||
25918|Garford Formation|69004|4|Described|iii,  p19, p28-p29, p32, p34-p35, p38|Miocene|Miocene|Eucla Basin. Alkaline lake deposits are common.|||Includes the Kingoonya Member.|Unconformably overlies the Pidinga Formation.|Oxidised sands, lacustrine calcareous clays and carbonates.|
25918|Garford Formation|69598|6|Mentioned|p9|Early Pliocene|Middle Miocene||||Includes the Kingoonya Member.|Overlain by the Narlaby Formation.||
25918|Garford Formation|69648|4|Described|p4, p6 Fig.3, p27-28, p32, map legend|Pliocene|Miocene|Tietkins Plain. Immature karst. Originally defined from Garford Palaeochannel on COOBER PEDY. Best exposures at Roadside Quarry and in two Tietkins wells nearby. Max thickness: likely <15 m. In lower part of formation (intersected in drillholes) locally ooid-rich mudstones, packstones and grainstone occur. Exact age arguable due to lack of diagnostic fossils.||Immarna Group||Unconformably overlies Hampton Sandstone and Pidinga Formation; overlain by Ilkina Formation.|Alkali, playa lake carbonates; lacustrine, argillaceous muds, carbonate mudstones; on OOLDEA dominantly calcareous/dolomitic mudstones and dolomite, palygorskite-rich argillaceous muds can occur near base; very little terrigenous clastic components.|
25918|Garford Formation|69649|5|Briefly described|p31-32, p48|Eocene|Eocene|Eucla Basin. Up to 100m thick. Lacustrine, flood-plain, lagoonal swamp and locally evaporative environments. Associated with sub-economic U mineralisation near contact with Pidinga Formation.||||Locally unconformably overlies Pidinga Formation.|Succession of oxidised, grey, green and cream, to black mud, minor carbonate and local basal and interbedded carbonaceous sand and grit.|
25918|Garford Formation|70397|5|Briefly described|p3|Middle Miocene|Middle Miocene|Eucla Basin. Equivalent stratigraphic level to Colville Sandstone and Nullabor Limestone.||Unit of Eucla Group.||Underlain by Wilson Bluff Limestone.||
25918|Garford Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||mudstone|
25918|Garford Formation|71317|4|Described|p137, p143-p144|Middle Miocene|Middle Miocene|Eucla Basin. Between 10 and 60m thick in places (not on Peltabinna). Deposited as lacustrine clay and fluviatile sand.||||Overlies the Pidinga Formation. Overlain by the Moornaba Sand. Equivalent to the Namba and Etadunna Formations.|Mudstone and minor horizons of silt and fine- to coarse-grained sand.|
25918|Garford Formation|71361|5|Briefly described|p5, p18|Middle Miocene|Early Miocene|Eucla Basin. Deposited in a lacustrine environment.||||||
25918|Garford Formation|71559|5|Briefly described|p19|Pleistocene|Miocene|Geological province: Gawler Craton.|||||Mudstone, carbonate, stomatolitic, oncolytic and oolitic, gastrapods, minor sandstone horizons. Upward change from argillaceous to carbonate mudstone. Lacustrine.|
25918|Garford Formation|71560|5|Briefly described|Map legend.|Pleistocene|Miocene|Lacustrine deposits.||Immarna Group.|||Mudstone, carbonate, stromatolitic, oncolytic and oolitic, gastropods, minor sandstone horizons. Upward change from argillaceous to carbonate mudstone.|
25918|Garford Formation|73099|5|Briefly described|Map legend.|Pliocene|Pliocene|Meramangye and Tallaringa Palaeochannels.||Immarna Group.||Overlies Pidinga Formation (Burdunga Subgroup).|Limestone and grey-green clayey sandstone and sandy claystone. Nodular, sheet and rubbly calcrete duricrust developed in palaeochannels.|
25918|Garford Formation|73100|5|Briefly described|Map legend|Pliocene|Miocene|||||Equivalent to Mangatitja Formation.|Lacustrine deposits of chalcedonic limestone and grey, green or red clayey sand to sandy clay.|
25918|Garford Formation|73108|5|Briefly described|Map legend.|Pleistocene|Eocene||||||Mudstone, carbonate, stromatolitic, oncolitic and oolitic, gastropods, minor sandstone horizons. Upward change from argillaceous to carbonate mudstone. Lacustrine.|
25918|Garford Formation|73109|5|Briefly described|Map legend.|Pliocene|Miocene|Subcrop and minor outcrop.||||Equivalent to Mangatitja Formation.|Lacustrine deposits of chalcedonic limestone and grey, green or red clayey sand to sandy clay. Calcareous regolith on top.|
25918|Garford Formation|73111|5|Briefly described|Map legend.|Pliocene|Miocene|Subcrop and minor outcrop.||||Equivalent to Mangatitja Formation.|Lacustrine deposits of chalcedonic limestone and grey, green or red clayey sand to sandy clay. Calcareous regolith on surface.|
25918|Garford Formation|73232|5|Briefly described|p8, p10|Pliocene|Miocene|Lacustrine palaeovalley infill. Well known from palaeovalleys along the Eucla Basin northern margin. One of the main stratigraphic units in palaeovalleys that trend southwards from the Musgrave Province across the Officer Basin to the Eucla Basin. [Approximately 58 m of mudstone and sandstone in drillhole DH1a from the Lindsay East Palaeovalley is attributed to this unit in Fig. 5 but not explicitly discussed in the text].|||||May include brown-black organic-, sulfidic- and clay-rich basal muds, olive-green muds, massive gypsum, and partly massive, moderately sorted, fine- to coarse-grained, quartz-rich sands and sandstones with intercalations of clay and gravel.|
23609|Garimala Limestone|13194|4|Described|p391 Tb. 4-16, p402 fig 4-66|Late Famennian|Late Famennian|Type Section: North of Surprise Creek 15o09'S 128o39'E. 150-340m thick marginal slope and reef margin facies.||Ningbing Group||Overlies Djilliri Limestone, Kamilili Formation, Wungabal Limestone (all unconformably). In subsurface, laterally equivalent to Kamilili Formation. Laterally equivalent to Buttons Formation.|Peloidal grainstone and limestone breccia, algal boundstone.|
23609|Garimala Limestone|40993|2|Defined|p9|Famennian|Famennian|||||||
23609|Garimala Limestone|41864|3|Fully described|p94|||||||||
23609|Garimala Limestone|41865|5|Briefly described|Map legend||late Famennian|||||||
23609|Garimala Limestone|41867|5|Briefly described|Map legend||late Famennian|||||||
23609|Garimala Limestone|42030|5|Briefly described|p750|||||||||
23609|Garimala Limestone|42933|5|Briefly described|Fig.94 p258|||||||||
23609|Garimala Limestone|64580|6|Mentioned|map legend|||Of Ningbing Group.||||||15-DEC-08
23609|Garimala Limestone|64694|5|Briefly described|p234 Fig.2|Late Devonian|Late Devonian|Carlton Shelf, Onshore Bonaparte Basin.||Unit in Ningbing Group.||||
23609|Garimala Limestone|69099|5|Briefly described|500k_geologyp08_lut.csv|Late Devonian|Late Devonian|||Ningbing Group||||
23609|Garimala Limestone|69165|6|Mentioned|500k_geologyp08_lut.csv|Famennian|Frasnian|||||||
23609|Garimala Limestone|69452|6|Mentioned|p36:7, 11|||Crops out in Ningbing Range.||Ningbing Group.||Stratigraphic equivalent of Buttons Formation.||12-JUL-16
23609|Garimala Limestone|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Ningbing Group.||||
23609|Garimala Limestone|69673|6|Mentioned|p169|||||Ningbing Group||Overlain by Buttons Formation, overlies Wungabal Limestone||
73578|Geemas Granodiorite|63441|5|Briefly described|p11 Tb. 2, p37|Archean|Archean|Of Indee Suite (Sisters Supersuite). Age: 2945+/-6Ma. Geological province: Pilbara Craton. Intrudes De Grey Supergroup.||||||07-FEB-11
73578|Geemas Granodiorite|70775|6|Mentioned|p65|||||Indee Suite||||
29206|Gibralter Quartz Monzonite|23785|5|Briefly described|p7|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
29206|Gibralter Quartz Monzonite|23788|5|Briefly described|p17|Archean|Archean|Geological Province: Yilgarn Craton||||||07-NOV-08
29206|Gibralter Quartz Monzonite|37296|6|Mentioned|p97|||||||||
29206|Gibralter Quartz Monzonite|39160|4|Described|p44|||Anal. geochemistry||||||
29206|Gibralter Quartz Monzonite|39317|5|Briefly described|p336|||See also Fig.2.||||||
29206|Gibralter Quartz Monzonite|40358|4|Described|p10|||||||||
29206|Gibralter Quartz Monzonite|40359|4|Described|p10|||||||||
29206|Gibralter Quartz Monzonite|40370|6|Mentioned|p10|||||||||
29206|Gibralter Quartz Monzonite|40903|6|Mentioned|p41|||||||||
29206|Gibralter Quartz Monzonite|43052|5|Briefly described|Fig.3.8|||||||||
29206|Gibralter Quartz Monzonite|50320|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Misspelling of Gibraltar Quartz Monzodiorite.||||||06-DEC-05
29206|Gibralter Quartz Monzonite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||quartz monzonite, alkali feldspar granite, syenite|
25921|Gibson Formation|13354|6|Mentioned|p375 Fig.6.|Late Cretaceous|Late Cretaceous|Unit of Bathurst Island Group. Overlies Woolaston Formation and underlies Puffin Formation.||91||||28-OCT-14
25921|Gibson Formation|41199|2|Defined|p13|late Quaternary|late Tertiary|Reserved as Gibson.||||||19-SEP-06
25921|Gibson Formation|50621|5|Briefly described|p159 Fig. 2|Cenozoic|Cenozoic|||||||19-NOV-08
25921|Gibson Formation|69297|6|Mentioned|p305|Santonian|Coniacian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin. ||Bathurst Island Group||Overlies the Woolaston Formation. Overlain by the Fenelon Formation.||
25921|Gibson Formation|69452|5|Briefly described|p36:15|Cretaceous|Cretaceous|Bonaparte Basin.||Bathurst Island Group.||||12-JUL-16
25921|Gibson Formation|70064|6|Mentioned|Northern p1-2|Late Cretaceous|Late Cretaceous|See also. Gas show in Abalone 1 and Abalone Deep 1 wells. Submarine fan sandstones are potential reservoirs.||||||12-JUL-16
81986|Gibson Honman Formation|72814|5|Briefly described|p201, Fig. 3, p202 Fig. 4|||East of Zuleika Shear, Ora Banda Domain.|||||Felsic dacitic volcanic and sedimentary rocks.|
83169|Gidji Lake Formation|73391|6|Mentioned|p246, 285, 420|||New unit name, suggested to include Grave Dam and Golden Valley members, the Gidji felsic unit, Gidji conglomerate and sandstone, and other rocks (listed). Named after the location where it is reasonably well exposed. Is presented more commonly as the informal Gidji Lake formation (vii-viii, p180, 194-195, 200, 244-245, 247, 304, 417, 419-421, 441-443, Appendices).|||||Includes wacke/sandstone.|
83169|Gidji Lake Formation|73596|6|Mentioned|p1159-1160, 1162|Neoarchean|Neoarchean|Kalgoorlie-Kambalda area. Mis-spelt as Gidgi on p1160.|2660 Ma.|Black Flag Group.||Overlies Gibson-Honman Formation. Is overlain by Merougil Formation.||
77223|Gifford Creek Carbonatite Complex|66299|4|Described|p20, pp305-308.|Neoproterozoic|Paleoproterozoic|Formerly Gifford Complex (Pearson et al. 1996); name changed for lack of alkaline igneous rocks other than carbonatite. Associated with U, REE and iron-oxide mineralisation. Accompanied by widespread alkaline metasomatism. Emplacement is probably related to shearing and faulting during Edmundian Orogeny.|Between 1619 Ma and 600 Ma.|||Sills, dykes and veins intrude Pimbyana and Yangibana Granites. Locally intrudes base of Edmund Group.|Ferroan carbonatites composed of predominantly ankerite-dolomite, magnetite, pyrochlore, arfvedsonite-riebeckite, and lesser calcite; associated with haloes and veins of fenitic alteration.|
77223|Gifford Creek Carbonatite Complex|67888|5|Briefly described|p47, p48|||Previously named Gifford Creek Alkaline Complex. Carbonatite intrusions include REE's and uranium minerals.|||||Carbonatite intrustions.|
77223|Gifford Creek Carbonatite Complex|69028|5|Briefly described|Map Legend|Stenian|Statherian|Mapped as 2 unnamed units.|1620-1030 Ma.||||Ferroan carbonatite, sills and dykes of Fe-carbonate, phlogopite, sodic amphibole, quartz; hematite-magnetite in places altered to massive goethite, fenitic alteration (K-feldspar, albite, sodic amphibole, cancrinite, pyrochlore, phlogopite).|06-MAY-14
77223|Gifford Creek Carbonatite Complex|69080|5|Briefly described|p686 Fig.4, p701|||Gascoyne Province. Appears in text as Gifford Creek Carbonatite Suite. Formerly Gifford Creek Complex. Hosts significant REE deposits in association with the Lyons River Fault.|< c.1620 Ma.|||Intrudes Pooranoo Metamorphics and Durlacher Supersuite.|A series of ferroan carbonatite sills, hydrothermally altered into mineralised ironstone veins and dykes.|
77223|Gifford Creek Carbonatite Complex|69237|6|Mentioned|p3|||Pirajno et al. (2010); formerly the Gifford Creek Igneous Complex. Renamed the Gifford Creek Ferrocarbonatite Complex (Pirajno and Gonzalez-Alvarez, 2013) in recognition of the preponderance of iron carbonate, in some cases exclusively.||||||
77223|Gifford Creek Carbonatite Complex|74493|4|Described|p1-3, p4 Fig.3, p6-7, p11-12, p16-20|Ectasian|Ectasian|Gascoyne Province, northeast region of the Mangaroon Zone. Abbreviated to GCCC. Contains a diverse range of alkaline magmatic and hydrothermal phases including some previously described rock types. Bounded to the south by the Lyons River Fault. Prospective for LREE mineralisation. Magnetite-biotite dykes and the ironstones of the complex are the most prospective. All rock types are mantled in fenites, present in the Pooranoo Metamorphics, Edmund Group and granitic host rocks. eNdt values range from -1.8 to -4. See also p5 Fig.4, p8 Fig.5, p10 Fig.8, p14, p15 Fig.12.|c. 1370 Ma||Lyons River Sills|Cuts the Yangibana Granite, Pimbyana Granite|Alkaline dyke and sill complexes. Includes dolomite and calcite carbonatites, ankerite-siderite carbonatites, magnetite-biotite dykes, and silica-rich alkaline veins. Alteration assemblages include ironstones, fenites, and glimmerites.|
77223|Gifford Creek Carbonatite Complex|74494|4|Described|p1007-1011, p1017, p1019-1024|Mesoproterozoic|Mesoproterozoic|Gascoyne Province. Abbreviated to GCCC. Occurs as thin sills and dykes along pre-existing structures. Emplaced in a transtensional/extensional, hypabyssal setting. Alteration is pervasive and envelopes all alkaline rock phases. Underwent multiple tectonic reworking events demonstrated by various monazite U-Pb and Sm-Nd ages (Zi et al., 2017; Slezak and Spandler, 2019). Hosts the ore of the Yangibana REE district, rich in Pr and Nd hosted mainly in monazite from ironstone dykes historically called ""ironstones"". Formation of the ironstone REE deposits from ankerite-siderite carbonatite is discussed, occasionally referred to as the Yangibana ironstones. Silica-rich alkaline veins are most abundant in the central region of the GCCC as a steeply dipping, N- to NNE-trending swarm. See also p1018 Fig.6.|1370 Ma||Lyons River Sills, Yangibana ironstones|Intrudes Durlacher Supersuite, Pooranoo Metamorphics, Edmund Group, Pimbyana Granite and Yangibana Granite.|Calcite and dolomite carbonatite dykes and sills, ankerite-siderite carbonate, magnetite-biotite dykes and silica-rich alkaline veins. Alteration phases include the Yangibana ironstones, fenites and glimmerites.|
69339|Gilbert's Grave granitoid|61144|5|Briefly described|p79-80, p82 Fig. 24|||See also Appendix D, p13-14.||||||
74611|Giles Suite|63864|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Warakurna Supersuite. Consists of  fine - to medium-grained metagabbro, gabbro, fine- to medium-grained biotite-bearing gabbro and undivided mafic-ultramafic intrusions.||||||11-SEP-08
74611|Giles Suite|64580|4|Described|map legend||Mesoproterozoic|Of Warakurna Supersuite. Layered mafic-ultramafic intrusions.||||||15-DEC-08
74611|Giles Suite|65898|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of Warakurna Supersuite.  Age of some units shown as >1078 Ma, others c.1075 Ma, c.1067 Ma. Divided into 24 unnamed units. Massive to layered gabbro, olivine gabbro, gabbronorite, troctolite. Mafic-ultramafic intrusions. Massive magnetitite, and dykes. ||||||
74611|Giles Suite|66280|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Unit in Warakurna Supersuite. Map area shows 24 unnamed units, mafic to ultramafic, including dunite, peridotite, orthopyroxenite, layered intrusions, troctolite, anorthosite, gabbronorites, olivine gabbros, amphibolites, mylonite. ||||||
74611|Giles Suite|66281|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|||Unit in Warakurna Supersuite.|||Olivine gabbro, metagabbro and metagabbronorite, gabbro and gabbronorite, olivine gabbro, leucotroctolite, anorthosite.|
74611|Giles Suite|66282|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|In this map area, is shown as comprising the Warakurna Supersuite. Is mapped as 32 un-named units of different lithologies, all mafic intrusive rocks.|>1078 - c.1075 Ma.|Unit in Warakurna Supersuite.|||Includes peridotite, pyroxenite, clinopyroxenite, mylonite from mafic intrusive rock, olivine gabbro, gabbronorite, leucogabbronorite, melagabbro, troctolite, anorthosite.|
74611|Giles Suite|66284|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Mapped as four separate but un-named units.||Unit in Warakurna Supersuite.|||Coarse- to medium-grained metagabbronorite; garnet-bearing amphibolite after gabbro; massive weakly metamorphosed gabbro cut by abundant quartz and pegmatite veins; ophitic to subophitic gabbro, locally foliated and mylonitic.|
74611|Giles Suite|67244|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Mapped as eleven separate but un-named sub-units.|1078 - 1074 Ma.|Unit in Warakurna Supersuite.|||Ophitic to sub-ophitic gabbro; mafic or weakly layered mafic intrusive rock; anorthosite to leucogabbroanorthosite; layered leucotroctolite; olivine gabbro; norite; metagabbro and metagabbronorite; leucogabbronorite sills, dykes and xenoliths.|
74611|Giles Suite|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Layered mafic-ultramafic intrusions. Mapped as 21 separate but un-named units.|>1078 - 1074 Ma.|Unit in Warakurna Supersuite.|||Includes anorthosite, leucotroctolite, gabbro, olivine-porphyritic metagabbro, gabbronorite, massive to foliated norite, mylonitic leucotroctolite, mylonite derived from mafic intrusive rock, magnetitite, olivine websterite, peridotite, pyroxenite.|
74611|Giles Suite|67375|4|Described|p38 Table 1, p159, p216, pp229-297.|Mesoproterozoic|Mesoproterozoic|At least 20 variably deformed and metamorphosed sheet-like bodies; 550 km E-W and 100 km N-S. Has considerable potential for Ni-Cu-PGE sulfide, and Fe-Ti-V oxide, mineralization.|c.1078 - c.1075 Ma.|Unit in Warakurna Supersuite.||Intrudes Kunmarnara Group and units of the Pitjantjatjara Supersuite. Is crosscut by Kullal Dyke Suite and Gairdner Dolerite.|Layered mafic-ultramafic intrusions of gabbro, troctolite, gabbronorite, norite, pyroxenite and anorthosite; massive gabbro and granite.|
74611|Giles Suite|67553|5|Briefly described|p40||||ca 1078-1071|Warakurna Supersuite|||Layered mafic-ultramafic intrusion, massive gabbro and granite.|06-AUG-19
74611|Giles Suite|68996|5|Briefly described|p7, 30-32, 33, 39,  65, 67, 68|Mesoproterozoic|Mesoproterozoic|Can be separated into two main groups (G1 & G2). Involved the injection of up to 42000km^3 of mantle material. G2 group ~1078 - 1065 Ma. See also pp41, 43, 45, 47, 48, 50, 61, 63.|1078 +/-3 Ma SHRIMP min age for G1 group||Includes Murray Range Gabbro, Bell Rock intrusion|G1 rocks intrude Kunmarnara Group.|Layered mafic and ultramafic intrusions; massive gabbros, troctolites,leucogabbronorites, gabbronorites, olivine gabbros, metagabbros. Density ranges from 2.92-3.46 g/cm^3.|17-JAN-17
74611|Giles Suite|69009|5|Briefly described|Map Legend|Stenian|Stenian|Contains 3 unnamed units, separately mapped.|> 1078-1075 Ma|Of the Warakurna Supersuite.|||Medium-grained, even textured gabbro - locally olivine porphyritic; medium-grained, even textured leucocratic gabbronorite - locally with troctolite, gabbronorite, olivine gabbro, and olivine norite; massive magnetite.|04-APR-14
74611|Giles Suite|69091|4|Described|p105, p106 Fig.5.7a,c, see comments|||Two gravity ridges correlate with outcrops. Voluminous mafic intrusions. Crystallisation age. Significant component of Giles Suite is made up of later stage massive gabbros, including Hinckley Gabbro. See also Giles Complex. See also p107 Fig.5.8a, p114, p115 Fig.5.14, p132, p134 Fig.6.2, p142-144, p146.|1076 +/- 7 Ma (U-Pb SHRIMP).|Warakurna Supersuite|Hinckley Gabbro.|Is overlain by Tollu Group and Bentley Supergroup.|Gabbros and mafic/ultramafic intrusions.|26-SEP-14
74611|Giles Suite|69152|5|Briefly described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|||Warakurna Supersuite|Includes Mount Holmes Gabbro|||
74611|Giles Suite|69153|5|Briefly described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Informally divided into Giles Suite 1 (layered mafic-ultramafic intrusions) and Giles Suite 2 (mafic intrusions).||Warakurna Supersuite|||Mafic-ultramafic intrusions (incl. leuco- and mela- variations): granite, (ferro)gabbronorite, olivine/biotite/magnetite-rich gabbro,  troctolite, dunite, pyroxenite, websterite, peridotite, norite, anorthosite, amphibolite, metagabbro, mylonite|
74611|Giles Suite|70134|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Warakurna Supersuite.||||
74611|Giles Suite|70153|5|Briefly described|100k_geologyp10_lut.csv|Mesoproterozoic|Mesoproterozoic|||Warakurna Supersuite|Includes Mount Holmes Gabbro.|||
74611|Giles Suite|70619|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Warkurna Large Igneous Province.|1078-1074 Ma|Warakurna Supersuite|||Amphibolite; gabbro; metagabbro.|
74611|Giles Suite|70763|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province. Two facies are mapped separately.|1068-1074 Ma.|Warakurna Supersuite.|||Cumulate-textured metagabbro, locally containing clinopyroxene, orthopyroxene, olivine and garnet; moderately to strongly foliated amphibolite after gabbro, strongly epidotized and cut by abundant quartz and pegmatite veins, locally mylonitic.|
74611|Giles Suite|70793|5|Briefly described|174761.1.pdf + other geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province. Of Warakurna Large Igneous Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Warakurna Supersuite Magmatic Event (1084-1040 Ma); Giles Event (1085-1040 Ma). Sample GSWA 174761 (porphyritic granite dyke) yielded an interpreted (weighted mean 207Pb*/206Pb*) magmatic crystallisation age of 1075+\-7 Ma.|1078-1074 Ma (inferred)|Unit of Warakurna Supersuite.||||
74611|Giles Suite|70826|6|Mentioned|p10|Mesoproterozoic|Mesoproterozoic|Musgrave Province. ||Warakurna Supersuite.||||20-MAY-20
74611|Giles Suite|70830|5|Briefly described|p3|Stenian|Stenian|This unit has an estimated length of 250km and volume of 25 000km^3.|c. 1070 Ma|||||
74611|Giles Suite|71210|5|Briefly described|p1, p4, p8-p13, p20-p21|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Comprises all igneous rocks formed during the Giles event. See also p51, p53, p79, p100, p108, p113-p114, p131, p133-p135.|c. 1078 Ma - 1076 Ma|Warakurna Supersuite|||Massive gabbros and associated felsic rocks.|
74611|Giles Suite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Of Warakurna Large Igneous Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Warakurna Supersuite Magmatic Event (1084-1040 Ma); Giles Event (1085-1040 Ma). Sample GSWA 174589 (metamorphosed quartz syenite) yielded weighted mean 207Pb/206Pb date of 1074+\-3 Ma, interpreted as the crystallization age of the quartz syenite dyke. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv.|1078-1074 Ma (inferred)|Unit of Warakurna Supersuite.|||Giles Suite 1: layered mafic-ultramafic intrusions of troctolite, norite, dunite, gabbro and metagabbro, anorthosite and clinopyroxeninite. Giles Suite 2: domianntly gabbro.|
74611|Giles Suite|71270|5|Briefly described|100k_geologyp10_lut.csv|||Of Warakurna Large igneous Province. ||Unit of Warakurna Supersuite.|Includes Mount Holmes Gabbro.|||
74611|Giles Suite|72242|5|Briefly described|p27,34|Stenian|Stenian|Geological province: Musgrave Province. Associated with Giles Event. Hosts the Nebo-Babel Ni-Cu PGE deposit in the western Mugrave Province. Temporally equivalent to Giants Head Suite.||||||
74611|Giles Suite|73437|5|Briefly described|p151|Mesoproterozoic|Mesoproterozoic|||Warakurna Supersuite|||Layered mafic-ultramafic intrusions. See also Giles intrusions p153.|
80998|Giles Suite 1|70793|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province. Of Warakurna Large Igneous Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Warakurna Supersuite Magmatic Event (1084-1040 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv.|1078-1075 Ma (inferred)|Unit of Warakurna Supersuite.|||Layered mafic-ultramafic intrusions; leucotroctolite, norite, gabbro and metagabbro, dunite, metagabbronorite, peridotite, pyroxenite, anorthosite, pyroxenite.|
80998|Giles Suite 1|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Informal subdivision of Giles Suite. Of Warakurna Large Igneous Province. Age inferred: 1078- 1075 Ma.||Warakurna Supersuite|Includes 2 unnamed subunits.||Layered mafic-ultramafic intrusions. Medium-grained, even-textured gabbro; locally olivine porphyritic. Cumulate-textured metagabbro; locally containing clinopyroxene, orthopyroxene, olivine and garnet.|
33668|Gilgarna Syenite|44202|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
33668|Gilgarna Syenite|69152|6|Mentioned|1m_geologyp08_lut.csv|Archean|Archean||||||Syenite; syenite group.|06-AUG-15
33668|Gilgarna Syenite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||syenite|
33668|Gilgarna Syenite|71270|5|Briefly described|1m_geologyp12_lut.csv|||Geological province: Yilgarn Craton, West Australian Craton. |||||Syenite|
41174|Gillam Monzogranite|50379|5|Briefly described|Map Legend|Archean|Archean|Of Yule Granitoid Complex. Geological Province: Pilbara Craton.||||||07-NOV-08
41174|Gillam Monzogranite|63441|5|Briefly described|p12 tb. 2|Archean|Archean|Of Split Rock Supersuite. Geological province: Pilbara Craton.||||||07-FEB-11
41174|Gillam Monzogranite|66108|5|Briefly described|Map legend|Neoarchean|Neoarchean|Unit in Split Rock Supersuite. Weakly feldspar-porphyritic biotite(-muscovite) monzogranite; locally with magnetite phenocrysts; massive to weakly foliated; weakly metamorphosed.||||||
41174|Gillam Monzogranite|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton. Age constrained by the parent Split Rock Supersuite.||Of the Split Rock Supersuite.|||Weakly feldspar-porphyritic biotite(-muscovite) monzogranite; locally with magnetite phenocrysts; massive to weakly foliated; weakly metamorphosed.|30-APR-14
41174|Gillam Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Weakly feldspar-porphyritic biotite(--muscovite) monzogranite; locally with magnetite phenocrysts; massive to weakly foliated; weakly metamorphosed.|
41174|Gillam Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; Split Rock Supersuite Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|2851-2831 Ma (inferred)|Unit of Split Rock Supersuite.|||Weakly feldspar-porphyritic biotite(-muscovite) monzogranite; locally with magnetite phenocrysts; massive to weakly foliated; weakly metamorphosed|
41174|Gillam Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
41174|Gillam Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Biotite(-muscovite) monzogranite, weakly feldspar-porphyritic; locally with magnetite phenocrysts; massive to weakly foliated; weakly metamorphosed.|
80956|Givetian-Frasnian reef complexes, marginal slope and basinal facies 80956|72034|5|Briefly described|500k_interpgeop16_lut|Frasnian|Givetian|Unnamed informal unit. Lennard Shelf, Canning Basin. Age: biostratigraphic.|||||Limestone, calcareous sandstone, and mudstone; common breccia and mass flow deposits; lesser siliciclastic sandstone and conglomerate.|
80957|Givetian-Frasnian reef complexes, platform facies 80957|72034|5|Briefly described|500k_interpgeop16_lut|Frasnian|Givetian|Unnamed informal unit. Lennard Shelf, Canning Basin. Age: biostratigraphic. Includes Pillara Limestone and Cadjebut Formation (reefal precursor).|||||Limestone with lesser siltstone and sandstone, commonly cyclic;|
42390|Gladstone Member|23815|5|Briefly described|p307|||Geological Province: Carnarvon Basin. Of the Carbla Oolite. Contains irreegular echinoids and molluscs.||||||
23618|Glass Hill Sandstone|22537|6|Mentioned|42|||Parent Mahoney Group||||||
23618|Glass Hill Sandstone|23621|5|Briefly described|p36|Devonian|Devonian|Of Mahony Group. Geological Province: Ord Basin.||||||
23618|Glass Hill Sandstone|23622|5|Briefly described|Map Legend|Devonian|Devonian|Of Mahony Group. Geological Province: Ord Basin.||||||
23618|Glass Hill Sandstone|40993|6|Mentioned|Fig.1|||||||||
23618|Glass Hill Sandstone|41598|5|Briefly described|p412|||||||||
23618|Glass Hill Sandstone|41811|6|Mentioned|p210|||Previously Elder Sandstone||||||
23618|Glass Hill Sandstone|41840|4|Described|p44|||||||||
23618|Glass Hill Sandstone|41864|3|Fully described|p56|||||||||
23618|Glass Hill Sandstone|41865|5|Briefly described|Map legend||Frasnian|||||||
23618|Glass Hill Sandstone|41866|5|Briefly described|Map legend|Frasnian||||||||
23618|Glass Hill Sandstone|42030|4|Described|p750|||||||||
23618|Glass Hill Sandstone|42821|5|Briefly described|p7|||||||||
23618|Glass Hill Sandstone|42829|6|Mentioned|p146|||||||||
23618|Glass Hill Sandstone|43299|5|Briefly described|Map Legend||Devonian|||||||
23618|Glass Hill Sandstone|43855|5|Briefly described|Map Legend||Frasnian|||||||
23618|Glass Hill Sandstone|44868|5|Briefly described|Map Legend||Frasnian|||||||
23618|Glass Hill Sandstone|60519|5|Briefly described|Map Legend|Frasnian|Frasnian|Geological Province: Ord Basin. Of the Mahony Group. Medium to fine grained quartz arenite; minor pebbly sandstone, conglomerate and siltstone.||||||05-NOV-04
23618|Glass Hill Sandstone|64580|6|Mentioned|map legend|||Of Mahony Group.||||||15-DEC-08
23618|Glass Hill Sandstone|65417|5|Briefly described|p165.|Frasnian|Frasnian|Hardman Sub-basin. Upward-coarsening fluvial deposits from uplift of the Osmand Range to the north.||||||
23618|Glass Hill Sandstone|67860|4|Described|p418 Tb.4-18, p422-423 Figs.4-88,89|Frasnian|Frasnian|Forms spectacular joint-controlled sandstone towers in Bungle Bungle Range. 200-1,000 m thick. Type section details given. Contains rare unidentified bivalve fossils. Also appears as Glasshill Standstone [!] in Fig.4-88.||Mahony Group||Unconformably overlies Goose Hole Group. Laterally equivalent to Boll Conglomerate and Purralili Sandstone.|Pebbly quartz sandstone; minor siltstone, conglomerate.|
23618|Glass Hill Sandstone|68656|6|Mentioned|GEOL_LUT_CSV/500k_geologyp08_lut|Frasnian|Frasnian|||Mahony Group||||
23618|Glass Hill Sandstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Frasnian|Frasnian|Ord Basin||Mahony Group|||Pebbly sandstone; minor siltstone and conglomerate.|31-JUL-15
23618|Glass Hill Sandstone|69165|5|Briefly described|100k_interpgeop_lut.csv|Frasnian|Frasnian|||Mahony Group|||Pebbly sandstone; minor siltstone and conglomerate.|
23618|Glass Hill Sandstone|69634|4|Described|100k_interpgeop_lut.csv|Frasnian|Frasnian|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny.|382.7-372.2 Ma (Biostrat)|Unit of Mahony Group.|||Pebbly sandstone; minor siltstone and conglomerate|
23618|Glass Hill Sandstone|70154|5|Briefly described|100k_interpgeop_lut.csv|||||Mahony Group|||Pebbly sandstone; minor siltstone and conglomerate.|
23618|Glass Hill Sandstone|71267|4|Described|GEOL_LUT_CSV files|Frasnian|Frasnian|Geological Province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny (450-295 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|382.7-372.2 Ma (biostrat)|Unit of Mahony Group.|||Medium- to fine-grained quartz arenite; minor pebbly sandstone, conglomerate and siltstone|
23618|Glass Hill Sandstone|73255|6|Mentioned|p534 Fig.2|Devonian|Devonian|||Mahony Group||Overlies the Buchanan Sandstone, underlies the Boll Conglomerate.||
77856|Gleesons Basalt|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2726 - 2680 Ma (inferred).|Coolgardie Subgroup|||Komatiitic basalt and shale; metamorphosed.|
77856|Gleesons Basalt|70326|4|Described|p360,364|Neoarchean|Neoarchean|Geological province: Coolgardie Domain, Kalgoorlie Terrane, Yilgarn Craton. Correlable to Bent Tree and big Dick basalts, and Redeemer and Burrell Well basalts.||||Underlain by Hampton Formation.|Basalt and high-Mg basalt.|
77856|Gleesons Basalt|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).  See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2726-2680 Ma (inferred)|Unit of Coolgardie Subgroup.|||Komatiitic basalt; metamorphosed; shale; metamorphosed.|
77856|Gleesons Basalt|73391|6|Mentioned|p194, 244, Appendices.|||Coolgardie Domain, Kalgoorlie Terrane. Appears as Gleeson's Basalt on p194, 244.||||Overlies Hampton Ultramafic. Is overlain by Talbot formation.||
77856|Gleesons Basalt|73596|6|Mentioned|p1162|||Coolgardie Inlier, Kalgoorlie Terrane.||Coolgardie Subgroup.||Overlies Hampton Hill Formation. Is overlain by Black Flag Group.||
74811|Glen Group|64891|5|Briefly described|p34 Fig.1, p37 Fig.2, p40-41, p48-9 Tb.1|Archean|Archean|Of the newly revised Murchison Supergp (Van Kranendonk 2008). Includes Ryansville and Wattagee Fms. Conformable on Polelle Group. Age: 2725-2700Ma. Geol.prov: Murchison Domain. Komatiitic basalt +underlying clastic sedim'y rocks; minor chert + rhyolite||||||07-FEB-11
74811|Glen Group|65548|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Murchison Supergroup, Youanmi Terrane, Yilgarn Craton. Includes the Watagee and Ryansville Formations.||||||
74811|Glen Group|66195|4|Described|p605, p599 Fig.2, p611 Fig.9|Neoarchean|Neoarchean||~2705 - 2710 Ma.|In Murchison Supergroup.||Overlies the Polelle Group.|Dominated by mafic and ultramafic rocks, also includes locally thick felsic volcanic units as well as banded iron formations and clastic sedimentary rocks.|13-MAR-12
74811|Glen Group|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Unit in Murchison Supergroup.|Includes Ryansville and Wattagee Formations.|||
74811|Glen Group|67129|4|Described|p17, p18 Fig.19, p19 Fig.20, p20, p27|Archean|Archean|See also p29, p35-36, p38-43, p51. Murchison Domain, Youanmi Terrane. Accompanied by widespread intrusion of synvolcanic granite plutons with common c.2950 Ma xenocrystic zircons indicating authochthonous development on older crust.|2735-2700 Ma|Murchison Supergroup|Includes Wattagee Formation, Ryansville Formation|Unconformably overlies Polelle Group, Yalgowra Suite|Coarse clastic sedimentary rocks, komatiitic basalt, minor rhyolite. Sandstone, shale, siltstone, chert pebble conglomerate, clast-supported boulder conglomerate.|07-SEP-17
74811|Glen Group|68107|6|Mentioned|p618, p619 Fig.8|Neoarchean|Neoarchean|Western Youanmi Terrane.|ca. 2724-2700 Ma|||||
74811|Glen Group|68108|5|Briefly described|p628, p651 Tb.4|Neoarchean|Neoarchean|NE Murchison Domain, Youanmi Terrane. U-Pb geochronology by Van Kranendonk & Ivanic (2008).|ca. 2735-2710 Ma||||Rhyolite, gabbroic sill.|
74811|Glen Group|68109|5|Briefly described|p659|Neoarchean|Mesoarchean|Murchison Domain.|ca. 2815-2710 Ma|Of the Murchison Supergroup.||||
74811|Glen Group|68110|3|Fully described|p672 Fig.1, p674, p687|Neoarchean|Neoarchean|Murchison Domain.|c. 2735 - 2700 Ma|Unit in Murchison Supergroup.|Includes Wattagee Formation and Ryansville Formation.|Overlies and intrudes Polelle Group.|Includes coarse clastic and finer-grained felsic volcaniclastic rocks; thick lower unit of pyroxene spinifex-textured komatiitic basalt and pillowed komatiitic basalt, locally interbedded with andesitic to rhyolitic volcanic rocks.|
74811|Glen Group|68561|5|Briefly described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. Metarhyolite dated. U-Pb zircon concordia age of 2725 +/- 4 Ma (MSWD = 0.97), interpreted as the age of magmatic crystallization of the rhyolite protolith. See geochron file 183975.1.pdf.||Of Murchison Supergroup|Includes Wattagee Formation, Ryansville Formation|||
74811|Glen Group|68698|5|Briefly described|p2, p4-5, p13, p18-19, p21|Neoarchean|Neoarchean|Final phase of greenstone development. At least 2km thick. c.2720 Ma. Emplacement was coeval with Yalgowra Suite.|2735-2710 Ma.|Murchison Supergroup.|Ryansville and Wattagee Formations.|Unconformably overlies Polelle Group.|Komatiitic-tholeiitic basalts.|
74811|Glen Group|69404|6|Mentioned|p4, p4 Fig.4|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. |2735 - 2710 Ma|||||
74811|Glen Group|69583|4|Described|p47, p49, p52-53, p126, p157; Plate 2|Mesoarchean|Mesoarchean|Murchison Domain. Deposition was coeval with emplacement of Yalgowra Suite. At least 2km thick.|c.2735-2710 Ma.|Murchison Supergroup.|Ryansville and Wattagee Formations.|Unconformably overlies the Polelle Group.||
74811|Glen Group|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean|||Murchison Supergroup|Ryansville Formation, Wattagee Formation|Overlies the Polelle Group||
74811|Glen Group|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Murchison Supergroup.|Ryansville, Wattagee Formations.|Unconformably overlies Polelle Group.||
74811|Glen Group|70020|4|Described|p117-118,130|Neoarchean|Neoarchean|Geological province: Yilgarn Craton. VHMS mineralisation occurs ar Gum Creek greenstone belt. Felsic volcanic rocks near the Bevan base metal occurrence yielded and age of 2722 +/- 6 Ma (Bodorkos et al, 2006).|2735-2700 Ma||Includes Ryansville and Wattagee formations.|Underlain unconformably by Polelle Group.|Felsic volcanic rocks and graphitic/carbonaceous sedimentary rocks.|16-JUL-19
74811|Glen Group|70030|4|Described|p190-192|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton.|ca. 2735-2700 Ma|Unit of Murchison Supergroup.|Includes Wattagee and Ryansville formation.|Uppermost unit of Murchison Supergroup.|Coarse clastic sedimentary rocks, komatiitic basalt and minor rhyolite.|
74811|Glen Group|70139|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.||Murchison Supergroup.|Wattagee Formation.|||
74811|Glen Group|70226|5|Briefly described|Map legend.|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Carton.|2735-2700 Ma||Mougooderra Formation|||16-DEC-15
74811|Glen Group|70418|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Murchison Supergroup.|Ryansville, Wattagee Formations.|||
74811|Glen Group|70419|6|Mentioned|p2|||Murchison Domain, Youanmi Terrane, Yilgarn Craton.||||||
74811|Glen Group|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton.|2735-2700 Ma.|Murchison Supergroup.|Mougooderra Formation.|||
74811|Glen Group|70796|4|Described|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. Affected by the Yilgarn Craton granite magmatism (3010  2600 Ma); Youanmi Terrane events (3131  2600 Ma). See also 100k_geologyl_lut.csv, 100k_geologyp_lut.csv. 100k_interpgeol_lut.csv, 100K_interpgeop_lut.csv,  500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 155568.1.pdf, 155572.1.pdf, 183975.1.pdf, 185922.1.pdf, 185925.1.pdf, 185927.1.pdf, 193972.1.pdf, 197420.1.pdf, 198295.1.pdf, 211101.1.pdf, Badja100_2240_stratig.pdf, Cue100_2443_stratig.pdf, Madoonga100_2444_stratig.pdf, MountMagnet100_2441_stratig.pdf, Reedy100_2543_stratig.pdf, Yalgoo100_2241_stratig.pdf. Numerous additional lithologies are provided.|ca 2735 to 2700 ma (inferred)|Murchison Supergroup|Includes the Ryansville Formation, Wattagee Formation and the Mougooderra Formation.|Coeval with the Yalgowra Suite.|Basalt, with underlying clastic sedimentary rocks; dominantly komatiitic basalt; minor rhyolite, andesite, and chert; weakly metamorphosed.|
74811|Glen Group|70826|6|Mentioned|p6 tbl 2, p8|Neoarchean|Neoarchean|Youanmi Terrane.||Murchison Supergroup||||22-APR-20
74811|Glen Group|70830|5|Briefly described|p5, p7-p9, p11-p12, p27-p28|Neoarchean|Neoarchean||c. 2735-2710 Ma||Includes the Ryansville Formation and the Wattagee Formation.|Unconformably overlies the Polelle Group. Coeval with Yalgowra Suite.||
74811|Glen Group|71148|6|Mentioned|p120|||Youanmi Terrane, Yilgarn Craton.||||||
74811|Glen Group|71168|4|Described|iii, p7-p8, p10|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. See also p25, p40 fig 25, p60.|c. 2735-2700 Ma||Includes the Ryansville Formation and the Wattagee Formation.|Unconformably overlies the Polelle Group.||
74811|Glen Group|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv.|2735-2700 Ma|Unit of Murchison Supergroup.|Includes Mougooderra Formation, Ryansville Formation, Wattagee Formation.|Coeval with Yalgora Suite and Big bell Suite.|Chert, banded chert and banded iron-formation; interlayered with tremolite schist derived from ultramafic intrusive rocks; basalt; massive to weakly foliated;  metamorphosed.|
74811|Glen Group|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|2735-2700 Ma.|Murchison Supergroup.|Wattagee Formation.||BIF, chert, jaspilite, shale, tremolite schist after ultramafic intrusive rocks, strongly foliated metabasalt and local amphibolite, massive to weakly foliated metabasalt.|
74811|Glen Group|71272|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|2735-2700 Ma.|Murchison Supergroup.|Mougooderra Formation.|||
74811|Glen Group|71809|5|Briefly described|map legend|Archean|Archean|Yilgarn Craton, Youanmi Terrane|~2735-2700 Ma|Of Murchison Supergroup.|Includes Mougooderra Formation.|||06-SEP-19
74811|Glen Group|72491|6|Mentioned|p5 Fig.4|||Murchison Terrane, Yilgarn Craton.||||||
74811|Glen Group|72494|5|Briefly described|p15, p17 Fig.3, p29|||Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c.2735 - 2700 Ma.|||Overlies Wilgie Mia Formation (Polelle Group).|Coarse clastic and finer-grained felsic volcaniclastic rocks; pyroxene-spinifex bearing volcanic rocks.|
74811|Glen Group|73023|5|Briefly described|p15|||Emplacement is consistent with lithospheric extension and onset of a mantle plume event across the Yilgarn Craton.|||||Includes komatiitic basalts.|
74811|Glen Group|73410|5|Briefly described|p13|||Mount Magnet area, Yilgarn Craton.|c.2735-2700 Ma.||Ryansville Formation.||Greenstone; ultramafic schists.|
74811|Glen Group|73453|5|Briefly described|p3|Neoarchean|Neoarchean|Youanmi Terrane (Murchison).|2800-2700 Ma||||Metasedimentary lithology, and mafic to felsic volcanics.|
74811|Glen Group|73596|5|Briefly described|p1165, 1169-1170|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane.|c.2730-2700 Ma.|Murchison Supergroup.|Ryansville, Wattagee, Marda, Diemans Formations; Dalgaranga Dolerite.|Overlies Polelle Group and, unconformably, Norie Group. Is intruded by Butcher Bird Monzogranite.|Sandstone and conglomerate with minor felsic lava, komatiitic basalt.|
40821|Glenayle Dolerite|24535|4|Described|p1, 2-19|Stenian|Stenian|Suite of dolerite sills, each usually > 100 m thick. Three types recognised - basaltic, doleritic and gabbroic. Intrudes Salvation Group. Age of intrusion: 1066+/-14 Ma (Pb-Pb). Dating and palaeomagnetism described.||||Intruded by Prenti Dolerite.||26-NOV-13
40821|Glenayle Dolerite|50188|5|Briefly described|p17|Neoproterozoic|Neoproterozoic|Age: c.800Ma. Intruded by dolerite dykes.||||||16-JUL-08
40821|Glenayle Dolerite|50195|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Fine- to medium-grained dolerite, intruded into the Salvation Group.  Age: c.1070Ma.||||||23-JUN-04
40821|Glenayle Dolerite|50222|5|Briefly described|p334 Tb.2|Mesoproterozoic|Mesoproterozoic|Mafic sills and dykes that intrude the Salvation Group.  Age: 1.07Ga.||||||
40821|Glenayle Dolerite|50226|6|Mentioned|p427, p434||Mesoproterozoic|Coeval with parts of Bangemall Supergroup.  Age: ~1.0 Ga.  Geological Province: northern margin of Earaheedy Basin.||||||
40821|Glenayle Dolerite|50319|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: c. 1070 Ma. Fine- to medium-grained dolerite. Intrudes the Scorpion and Salvation Groups.||||||28-MAY-04
40821|Glenayle Dolerite|62453|6|Mentioned|p70|||Age: 1070Ma. ||||||
40821|Glenayle Dolerite|63022|6|Mentioned|p1019 Fig. 5|||||||||
40821|Glenayle Dolerite|63866|4|Described|p163, p178|Stenian|Stenian|Eastern Bangemall Basin. K-Ar dates are from K-feldspars and are interpreted as minimum estimates of the time of dolerite crystallisation. Ages are derived from Nelson, 2002. Wingate obtained U-Pb SHRIMP baddeleyite intrusive ages of 1066 +/- 14 Ma and 1068 +/- 20 Ma for this unit which is interpreted as the best estimate for the age of this unit. Nelson also reported a K-Ar whole rock age of 1058 +/- 13 Ma for a basalt.|917 +/- 13 Ma and 968 +/- 19 Ma ||||Dolerite and basalts.|
40821|Glenayle Dolerite|64572|6|Mentioned|p810 Fig. 10|Neoproterozoic|Neoproterozoic|Age: ca. 1066Ma (U-Pb).||||||22-DEC-08
40821|Glenayle Dolerite|64580|4|Described|map legend||Mesoproterozoic|Of Warakurna Supersuite. Dolerite sill, dyke, and plug; fine- to coarse-grained dolerite.||||||15-DEC-08
40821|Glenayle Dolerite|64655|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes Weld Spring, Parker Range and Yallum Hill Members. Fine- to medium-grained dolerite.||||||
40821|Glenayle Dolerite|64772|4|Described|p13, Plate 1, p15|Mesoproterozoic|Mesoproterozoic|Part of Warakurna Large Igneous Province. Includes Weld Spring, Parker Range + Yallum Hill Members. Age: 1066+/-14Ma SHRIMP baddeleyite. Intrudes Salvation Group. Dolerite (microgabbro) sills; dyke + plug, fine-to coarse-grained dolerite.|several SHRIMP U-Pb baddleyite and zircon ages|||Intrudes Salvation Group and parts of Earaheedy Group; intruded by Prenti Dolerite|dolerite (microgabbro) sills: typically clinopyroxene (50-55 vol.%) and labradorite (30-35 vol.%), with accessory ilmenite, titanomagnetite, and apatite.|25-NOV-13
40821|Glenayle Dolerite|65369|5|Briefly described|p35|||Of the Bangemall Supergroup, Western Australia. Intraplate (flood-type) basalts.||||||19-MAR-12
40821|Glenayle Dolerite|65899|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age shown as c.1070 Ma. Unit in Warakurna Supersuite. Shown as combined Glenayle and Prenti Dolerites, with one description: Dolerite sill, dyke and plug; fine- to coarse-grained dolerite.||||||
40821|Glenayle Dolerite|66256|6|Mentioned|p17 Fig.13|||||||||
40821|Glenayle Dolerite|66427|6|Mentioned|p41 Tb.1, p42, p44-45  |||Part of the Warakurna Large Igneous Province. Mis-spelt as Glenyale on p44 and 45. May be 3-4 km thick; individual sills are up to 100m.|1076 Ma.|||Intrudes Salvation Group.|Mafic dykes and sills.|
40821|Glenayle Dolerite|67128|6|Mentioned|p5 Fig.4|||Warakurna Large Igneous Province.||||||
40821|Glenayle Dolerite|67375|5|Briefly described|p14 Fig.9, p229.|||Part of the Warakurna Large Igneous Province. On the northern margin of the Earaheedy Basin,a sill complex extending about 150 km ESE and about 60 km to the north. Individual sills up to 100 m thick; total thickness may be 3 - 4 km.||||||
40821|Glenayle Dolerite|67553|6|Mentioned|p15|||Of Earaheedy Basin, part of the Warakurna Large Igneous Province.||||||
40821|Glenayle Dolerite|69003|5|Briefly described|p4, p50 Fig.59, p53|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen. Part of the c.1070 Ma Warakurna LIP.|c.1070 Ma.|||Intrudes Salvation Group.||
40821|Glenayle Dolerite|69091|5|Briefly described|p202, p203|||Glenayle Dolerite sills intrude Earaheedy Basin, Collier Basin and Salvation Basin. Presented as Glenayle dolerite on p202, once.|ca. 1070 Ma|||||
40821|Glenayle Dolerite|69152|5|Briefly described|GEOL_LUT_CSV files + geochron files|Stenian|Stenian|Grouped as Glenayle and Prenti Dolerites||Warakurna Supersuite|||Fine to medium grained dolerite sills and dykes.|06-AUG-15
40821|Glenayle Dolerite|70153|4|Described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|See also 100k_geologyp14_lut.csv and 500k_interpgeop14_lut.csv. Shown as parent unit of Prenti Dolerite [in which case the latter should be named Prenti Dolerite Member].|||Includes Prenti Dolerite|||
40821|Glenayle Dolerite|70316|6|Mentioned|p120|||Warakurna LIP.|1068 +/- 20 Ma; 1063 +/- 21 Ma.|||||
40821|Glenayle Dolerite|71210|6|Mentioned|p5, p11|||||Warakurna Supersuite||||
40821|Glenayle Dolerite|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||dolerite|
40821|Glenayle Dolerite|71270|5|Briefly described|1m_geologyp12_lut.csv|||Of Warakurna Large Igneous Province. See 1m_geologyp12_lut.csv, 100k_interpgeol_lut.csv.|||||Fine to medium grained dolerite sills and dykes.|
40821|Glenayle Dolerite|72034|6|Mentioned|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Prenti Dolerite.|||
25926|Glidden Group|22716|6|Mentioned|p237|Ectasian|Ectasian|Age: 1250 Ma. Regarded as equivalent to shallow marine deposits of Victoria River Basin.||||||
25926|Glidden Group|22754|4|Described|p11 Tb. 3|Mesoproterozoic|Mesoproterozoic|||||||
25926|Glidden Group|23383|6|Mentioned|p20|||Overlain unconformably in places by Louisa Downs Group rocks.||||||25-JAN-05
25926|Glidden Group|23599|6|Mentioned|p17|||Overlying unit Louisa Downs Group||||||
25926|Glidden Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
25926|Glidden Group|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
25926|Glidden Group|31393|6|Mentioned|Pl.25|||||||||
25926|Glidden Group|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
25926|Glidden Group|32660|4|Described|Table 6|||||||||
25926|Glidden Group|32728|4|Described|p43|||See also P44||||||
25926|Glidden Group|36551|6|Mentioned|Table 10|||||||||
25926|Glidden Group|36885|4|Described|p178|||See also P177.||||||
25926|Glidden Group|36888|6|Mentioned|p213|||||||||
25926|Glidden Group|36898|6|Mentioned|p183|||||||||
25926|Glidden Group|37299|6|Mentioned|Fig.1|||||||||
25926|Glidden Group|37462|4|Described|Table 4.VI|||See also P253||||||
25926|Glidden Group|37927|6|Mentioned|p511|||||||||
25926|Glidden Group|38157|6|Mentioned|p282|||||||||
25926|Glidden Group|38988|6|Mentioned|Fig.4|||||||||
25926|Glidden Group|43666|6|Mentioned|p7|||||||||
25926|Glidden Group|44155|5|Briefly described|p232, p250-251, p254 Fig.3-40|Mesoproterozoic|Mesoproterozoic||||Harms and Forman Sandstones; Matheson and Maddox Formations.|Overlies Carson Volcanics unconformably. Overlies Hooper Complex and Lamboo Complex (both unconformably). Correlated with Glenhill Formation. Is overlain unconformably by Kuniandi Group.|Sandstone, shale and siltstone.|
25926|Glidden Group|44231|5|Briefly described|Map Legend|Neoproterozoic|Mesoproterozoic|Includes the Harms Sandstone, and the Matheson, Forman and Maddox Formations. Geological Province: Glidden Basin.||||||22-MAY-08
25926|Glidden Group|44397|14|Not recorded|p.6,9,15,19,Fig4,Tb3||Adelaidean|Defn. on Tech.File E/52-9.||||||
25926|Glidden Group|44398|14|Not recorded|map legend||Adelaidean|||||||
25926|Glidden Group|44867|5|Briefly described|Map Legend||Mesoproterozoic|||||||
25926|Glidden Group|45047|4|Described|p34|||?Adelaidean. See P35.||||||
25926|Glidden Group|48927|2|Defined|p6|Adelaidean|Adelaidean|||||||
25926|Glidden Group|50225|5|Briefly described|p406 Fig. 10, p407|Mesoproterozoic|Mesoproterozoic|Geological Province: Kimberley Basin.||||||07-FEB-11
25926|Glidden Group|64580|4|Described|map legend|Mesoproterozoic|Mesoproterozoic|Sandstone, quartz wacke, shale, and siltstone.||||||09-DEC-08
25926|Glidden Group|68244|6|Mentioned|p666|Mesoproterozoic|Mesoproterozoic|||||Overlain unconformably by Louisa Downs Group.||
25926|Glidden Group|69099|5|Briefly described|500k_geologyp08_lut.csv|Mesoproterozoic|Mesoproterozoic||||||Sandstone, quartz wacke, shale, and siltstone.|31-JUL-15
25926|Glidden Group|69165|4|Described|500k_geologyp08_lut.csv|Mesoproterozoic|Mesoproterozoic||||||Undivided; sandstone, quartz wacke, shale and siltstone|
25926|Glidden Group|69634|5|Briefly described|500k_geologyp08_lut.csv|Mesoproterozoic|Mesoproterozoic||||||Undivided; sandstone, quartz wacke, shale, and siltstone|
25926|Glidden Group|70154|5|Briefly described|500k_interpgeop14_lut.csv|Mesoproterozoic|Mesoproterozoic||1000-1600 Ma||||Sandstone, quartz wacke, shale, and siltstone|
25926|Glidden Group|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Glidden Basin.||||||
25926|Glidden Group|70851|6|Mentioned|p19|||||||||
25926|Glidden Group|71267|4|Described|GEOL_LUT_CSV files|||Geological Province: Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|1797-635 Ma (Inferred-biostrat)||Includes Forman Sandstone, Harms Sandstone, Maddox Formation, Matheson Formation.||Sandstone, quartz wacke, shale, and siltstone.|
25926|Glidden Group|72034|5|Briefly described|500k_interpgeop16_lut|Cryogenian|Paleoproterozoic|Glidden Basin.|||||Sandstone, quartz wacke, shale, and siltstone.|
74830|Gnanagooragoo Igneous Complex|64891|5|Briefly described|p37 Fig. 2, p44, p52-53 Tb. 1|Archean|Archean|Of the Yalgowra Suite. Age: c. 2730Ma. Geological province: Murchison Domain. Layered dolerite, gabbro, wehrlite, and olivine-chromite cumulate rocks; metamorphosed.||||||05-AUG-11
74830|Gnanagooragoo Igneous Complex|65548|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Yalgowra Suite, Youanmi Terrane, Yilgarn Craton. Includes unnamed high grade metamorphics, mafic and some ultramafic intrusives; deformed and metamorphosed.||||||
74830|Gnanagooragoo Igneous Complex|66195|4|Described|p605, p598 Fig.1, p599 Fig.2, p602 Fig.4|Neoarchean|Neoarchean|Cut by c.2740 Ma felsic igneous rocks and intrudes ~2960 Ma (and possibly 2752 Ma) felsic volcaniclastics.|~2745 Ma.|||Unconformably overlain by the Glen Group.|Lower zone: peridotite including dunite-harzburgite-lherzolite, wehrlite (~500m thick). Main zone: gabbro (~200m thick). Upper zone: dolerite (~500m thick).|13-MAR-12
74830|Gnanagooragoo Igneous Complex|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Unit in Annean Supersuite.|||Dolerite, medium-grained with local fine- and coarse-grained layers; massive, locally weakly deformed; metamorphosed.|
74830|Gnanagooragoo Igneous Complex|67129|6|Mentioned|p18 Fig.19, p20, p29, p39, p52, p54|Archean|Archean|Murchison Domain, Youanmi Terrane. Peridotite hosts PGE, Au, Ni and Co mineralisation.|~2745 Ma|Annean Supersuite.||Intrudes Wilgie Mia Formation|A large, layered igneous complex: peridotite, dolerite and gabbro.|07-SEP-17
74830|Gnanagooragoo Igneous Complex|68108|5|Briefly described|p651 Tb.4|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane.|ca 2750 Ma; U-Pb (Ivanic et al. 2010).||||Differentiated igneous complexes.|
74830|Gnanagooragoo Igneous Complex|68110|5|Briefly described|p672 Fig.1, p687|Neoarchean|Neoarchean|Time of emplacement apparently between Polelle Group and Glen Group.|< ca 2740 +/- 7 Ma|||||
74830|Gnanagooragoo Igneous Complex|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. Metadolerite U-Pb zircon age: 2805 +/- 19 Ma tentatively interpreted as the age of an older source rock from which the zircons were derived, and therefore a maximum age for dolerite crystallization. From geochron file 194757.1.pdf.|2750-2735 Ma|Annean Supersuite|Includes 3 unnamed subunits|Gabbros cut by 2741 +/- 7 Ma porphyritic microgranites and are unconformably overlain by the Ryansville Formation of the 2735-2710 Ma Glen Group.|Dolerite; Ultramafic intrusive rock; Wehrlite; metamorphosed and/ or serpentinized.|
74830|Gnanagooragoo Igneous Complex|68698|5|Briefly described|p4-5|Neoarchean|Neoarchean|Emplaced below and within the BIF units of the Wilgie Mia Formation in the Weld Range. Maximum age from a tuff unit; minimum age from a cross-cutting granite.|2752 Ma to c.2740 Ma.|||Intrudes the coeval Wilgie Mia Formation.|A thick, differentiated mafic-ultramafic intrusion.|
74830|Gnanagooragoo Igneous Complex|69583|4|Described|p47,p49-50,p98,p102,p126,p177; Plate 2|||Not assigned to a mafic-ultramafic suite. Coevally emplaced below, and within the BIF component of, the Wilgie Mia Formation (Polelle Group). Age limits from a crystal tuff unit and cross-cutting intrusion respectively. Also appears on p47 mis-spelt as Gnanagooraroo. Igneous stratigraphic column.|Between c.2785 Ma  and c.2735 Ma.|Annean Supersuite.||Underlies and intrudes the Wilgie Mia Formation.|A thick, differentiated mafic-ultramafic intrusion: funnel-shaped at lower levels, and thick sheeted sills of homogeneous gabbro and dolerite at higher levels.|
74830|Gnanagooragoo Igneous Complex|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean|||||||
74830|Gnanagooragoo Igneous Complex|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||||||
74830|Gnanagooragoo Igneous Complex|70332|6|Mentioned|p77, 81|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Has similar lithologies to the Narndee Igneous Complex.|<2807 Ma (Wingate et al., 2012).|||||
74830|Gnanagooragoo Igneous Complex|70419|6|Mentioned|p2, p7-8|||Wang (1998). Murchison Domain, Youanmi Terrane, Yilgarn Craton. Lacks the distinctive magnetitite units in the upper zone that characterise the Meeline Suite igneous complexes.||||||
74830|Gnanagooragoo Igneous Complex|70796|4|Described|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. Affected by the Yilgarn Craton granite magmatism (3010  2600 Ma); Youanmi Terrane events (3131  2600 Ma). See also 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 194757.1.pdf, Madoonga100_2444_stratig.pdf.|2752 +/ 9 Ma to 2740 +/ 7 Ma (isotopic)|Annean Supersuite|||Layered dolerite, gabbro, wehrlite, and olivinechromite cumulate rocks; metamorphosed|
74830|Gnanagooragoo Igneous Complex|70826|6|Mentioned|p8|Neoarchean|Neoarchean|western Yilgarn Craton.||||||
74830|Gnanagooragoo Igneous Complex|70830|5|Briefly described|p2, p4-p5, p7, p27, p55|Neoarchean|Neoarchean||c. 2752-2740 Ma|||Intrudes the Wilgie Mia Formation.|Ultramafic cumulate rocks and thick, sheeted sills of homogeneous gabbro and dolerite.|
74830|Gnanagooragoo Igneous Complex|71311|6|Mentioned|p794|||Northern Youanmi Terrane, Yilgarn Craton.||||||
74830|Gnanagooragoo Igneous Complex|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Youanmi Terrane. 3 unnamed subunits shown.|||||Dolerite, medium grained; local fine- + coarse-grained layers. Gabbro, coarse grained; alternating layers melanocratic/leucocratic gabbro. Both massive, locally weakly deformed; metamorphosed. Ultramafic intrusive rock; metamorphosed; serpentinized.|
78990|Gnows Nest Granodiorite|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton.|c.2951 Ma.|Thundellara Supersuite.|||Metamorphosed granodiorite to tonalite with K-feldspar phenocrysts up to 8mm in 4-6mm matrix. A separately-mapped sub-unit is similar, but also contains hornblende phenocrysts.|
78990|Gnows Nest Granodiorite|70796|4|Described|100k_geologyp_lut.csv|Mesoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. See also 100K_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 155879.1.pdf, 203702.1.pdf, 203703.1.pdf, Badja100_2240_stratig.pdf. Numerous additional lithologies are discussed.|ca 2958 Ma (inferred)|Thundelarra Supersuite||Intrudes the Gossan Hill Formation.|Metamorphosed granodiorite to tonalite with Kfeldspar phenocrysts up to 8 mm in 46 mm matrix|
78990|Gnows Nest Granodiorite|71269|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.|2951 Ma (inferred)|Unit of Thundelarra Supersuite.||Intrudes into base of Gossan Hill Formation. May be subvolcanic to Scuddles Member.|Metamorphosed tonalite to granodiorite with hornblende and K-feldspar phenocrysts up to 8 mm in 4-6 mm matrix.|
78990|Gnows Nest Granodiorite|71272|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c.2951 Ma.|Thundelarra Supersuite.|||Metamorphosed granodiorite to tonalite with K-feldspar phenocrysts up to 8mm in 46mm matrix.|
30178|Goat Dam Monzogranite|43148|5|Briefly described|map legend||Archean|||||||07-NOV-08
30178|Goat Dam Monzogranite|43222|5|Briefly described|map legend||Archean|||||||07-NOV-08
30178|Goat Dam Monzogranite|43294|4|Described|p8||Archean|||||||07-NOV-08
30178|Goat Dam Monzogranite|43497|5|Briefly described|11|||||||||
30178|Goat Dam Monzogranite|44202|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
30178|Goat Dam Monzogranite|60076|5|Briefly described|p45 App. 1|||[Agmgd]   Equigranular biotite monzogranite.||||||
30178|Goat Dam Monzogranite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Equigranular biotite monzogranite; strongly deformed mafic enclaves locally.||||||07-FEB-11
30178|Goat Dam Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Equigranular biotite monzogranite; strongly deformed mafic enclaves locally.|06-AUG-15
30178|Goat Dam Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Equigranular biotite monzogranite; strongly deformed mafic enclaves locally.|
30178|Goat Dam Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
30178|Goat Dam Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. See 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|||||Equigranular biotite monzogranite; strongly deformed mafic enclaves locally|
38758|Gobbos Granodiorite|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Age: 3314+/-4Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
38758|Gobbos Granodiorite|63417|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite.  Age: 3313Ma. Geological Province: Pilbara Craton. Biotite granodiorite and monzogranite with minor hornblende; medium-grained, seriate to locally porphyritic, metamorphosed.||||||07-NOV-08
38758|Gobbos Granodiorite|63441|5|Briefly described|p8 Tb. 2|Archean|Archean|Of Emu Pool Supersuite. Age: 3313+/-4Ma.  Geological province: Pilbara Craton.||||||07-FEB-11
38758|Gobbos Granodiorite|64580|4|Described|map legend||Paleoarchean|Of Emu Pool Supersuite. Biotite granodiorite and monzogranite, with minor hornblende; medium grained, seriate to locally porphyritic; weakly metamorphosed.||||||08-DEC-08
38758|Gobbos Granodiorite|64653|5|Briefly described|Map Legend|Archaean|Archaean|Geological Province: Pilbara Craton. Biotite granodiorite and monzogranite with minor hornblende; medium grained, seriate to locally prophyritic; metamorphosed.||||||07-FEB-11
38758|Gobbos Granodiorite|65008|4|Described|p5, p7, p8, p12, p15, p15 Tb.1, p26, p41|Paleoarchean|Paleoarchean|East Pilbara Granite-Greenstone Terrane. Geochronology by: M.E. Barley, and N.J McNaughton, 1998, Precambrian Research, v.96, p.41-62. Hosts Cu-Mo-W(-F) deposits and occurrences.|3313 Ma|||Intrudes the Warrawoona Group.|Biotite granodiorite and monzogranite with minor hornblende; medium grained, seriate to locally porphyritic; metamorphosed.|
38758|Gobbos Granodiorite|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.|c.3313 Ma (Barley and Pickard 1999).||||Biotite granodiorite and monzogranite, with minor hornblende, medium-grained, seriate to locally porphyritic; quartz-plagioclase porphyry of dacitic composition.|
38758|Gobbos Granodiorite|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c.3313 Ma (Barley and Pickard 1999).|Of Emu Pool Supersuite.|||Biotite granodiorite and monzogranite, with minor hornblende, medium-grained, seriate to locally porphyritic; porphyritic quartz-plagioclase microgranodiorite, minor hornblende. All metamorphosed.|
38758|Gobbos Granodiorite|65827|3|Fully described|p6 Tb.2, p9 Fig 3, p11, p21, p24, p45,|Paleoarchean|Paleoarchean|Of Emu Pool Supersuite. Intrudes Euro Basalt. Seriate to locally porphyritic, grey granodiorite and monzogranite with phenocrysts of plagioclase, quartz, biotite, minor hornblende. 3313 +/- 4 Ma SHRIMP U-Pb zircon (Barley and Pickard 1999). Associated with Cu-Mo mineralisation.||||||
38758|Gobbos Granodiorite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Age derived from quartz-porphyritic intrusive rhyolite or microgranite sample (180067.1.pdf)|3313 +/- 3 Ma (SHRIMP)|Emu Pool Supersuite|||Biotite granodiorite and monzogranite; weakly metamorphosed. Fine grained metagranite, quartz monzonite to granodiorite, porphyritic quartz-plagioclase microgranodiorite. Monzogranite and granodiorite, biotite tonalite; all metamorphosed.|
38758|Gobbos Granodiorite|69185|4|Described|GEOL_LUT_CSV files||Paleoarchean|Geological province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 3317-3307 Ma|Unit of Emu Pool Supersuite.|||Biotite granodiorite and monzogranite, with minor hornblende; medium grained, seriate to locally porphyritic; weakly metamorphosed|
38758|Gobbos Granodiorite|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA 180067 (metamorphosed microgranite) yielded an interpreted igneous crystallisation age of 3313+\-3 Ma for the granite (weighted mean 207pb/206Pb).See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_geologyp08_lut.csv.|3314 Ma (isotopic, inferred)|Unit of Emu Pool Supersuite.||Intrudes into Euro Basalt.|Biotite granodiorite and monzogranite, with minor hornblende; biotite tonalite, quartz-plagioclase microgranodiorite.|
38758|Gobbos Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite, monzogranite|
38758|Gobbos Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||3313+/-4 Ma|Emu Pool Supersuite|||Biotite granodiorite and monzogranite, with minor hornblende; medium grained, seriate to locally porphyritic; weakly metamorphosed.|
79348|Golden Cities Granodiorite|70482|6|Mentioned|p317, 320, 330, 332-333|Neoarchean|Neoarchean|Occurs in the centre of the Scotia-Kanowna Dome batholith, Eastern Goldfields Superterrane, Eastern Yilgarn Craton. Hosts the Woodcutters camp. In most cases, appears in the text as Golden Cities granodiorite.|2656 +/- 3 Ma (Cassidy et al., 2002).||||Textured, Mafic-type. Hornblende-biotite bearing; also thin aplite veins/dykes and more mafic, finer grained granodiorite dykes.|
79348|Golden Cities Granodiorite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|3010-2600 Ma (inferred)||||Fine- to medium-grained granodiorite|
37550|Golden Eagle Orthogneiss|50287|5|Briefly described|Map Legend|Archean|Archean|Of Kurrana Granitoid Complex. Age: c. 3178 Ma. Geological Province: Kurrana Terrane, Pilbara Craton.||||||07-NOV-08
37550|Golden Eagle Orthogneiss|61253|5|Briefly described|p56, p54-55 Fig. 3|Archean|Archean| Age: c.3178Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
37550|Golden Eagle Orthogneiss|63417|5|Briefly described|Map legend|Archean|Archean|Of Mount Billroth Supersuite.  Age: 3199-3178Ma. Geological Province: Pilbara Craton. Layered orthogneiss derived from tonalite, granodiorite, monzogranite and pegmatite; includes layers and lenses of amphibole and ultramafic schist.||||||07-NOV-08
37550|Golden Eagle Orthogneiss|63441|5|Briefly described|p9 Tb. 2, p35|Archean|Archean|Of the Mount Billroth Supersuite. Ages: 3178+/-3Ma and 3199+/-3Ma. Geological province: Kurrana Terrane/Pilbara Craton.||||||07-FEB-11
37550|Golden Eagle Orthogneiss|63854|5|Briefly described|p230|Mesoarchean|Mesoarchean|Kurrana Terrane.|ca. 3199-3178 Ma||||Strongly deformed, amphibolite facies, lithologically layered orthogneiss consisting of foliated protoliths of biotite-bearing monzogranite, granodiorite and tonalite interlayered with lenses of amphibolite, ultramafic schist and quartz-mica schist.|
37550|Golden Eagle Orthogneiss|64654|5|Briefly described|Map Legend|Archaean|Archaean|Of Mount Billroth Supersuite.  Age: 3199-3178Ma. Geological Province: Pilbara Craton. Layered orthogneiss derived from tonalite, granodiorite, monzogranite, and pegmatite; includes layers and lenses of amphibolite and ultramafic schist.||||||
37550|Golden Eagle Orthogneiss|64656|5|Briefly described|Map Legend|Archaean|Archaean|Of Mount Billroth Supersuite. Age: 3199-3178Ma. Geological Province: Kurrana Terrane (Pilbara Craton). Layered orthogeniss derived from tonalite, granodiorite, monzogranite and pegmatite; incl. layers and lenses of amphibolite and ultramafic schist.||||||
37550|Golden Eagle Orthogneiss|65008|4|Described|p7, p16, p18, p19, p21, p28, p41|Mesoarchean|Mesoarchean|Geochronology by: D.R. Nelson, in prep, GSWA Record 2004/2. Contains Cu-Pb-Zn mineral occurrences at Coondoon and Coondamar Creek. Of the Kurrana Granitoid Complex, Kurrana Terrane.|3199-3178 Ma|||Intrudes the Bonney Downs Granite.|Layered orthogneiss derived from monzogranite, granodiorite, tonalite and pegmatite; alternating biotite and feldspar-rich layers: includes layers and lenses of amphibolite and ultramafic schist.|
37550|Golden Eagle Orthogneiss|65825|4|Described|p6, p7 Fig.4, p12, p16, p32.|||Multiply deformed and foliated. Appendix 2 shows this as a unit in the Mount Billroth Supersuite, according to the GSWA databases.|Granite precursor 3225 - 3178 Ma (Nelson 2005).|Unit in Kurrana Granitic Complex.||Is intruded by Bonney Downs Granite. Is unconformably overlain by Fortescue Group.|Strongly foliated layered orthogneiss; tectonically interleaved with amphibolite and pelitic and ultramafic schists; extremely weathered. In adjacent map areas, includes metamorphosed biotite-bearing monzogranite, granodiorite, and tonalite.|
37550|Golden Eagle Orthogneiss|65828|5|Briefly described|Map legend|Archean|Archean||c.3178 Ma (Nelson 2004).|Unit in Kurrana Granitoid Complex.||Locally interleaved with Coondamar Formation.|Layered orthogneiss derived from monzogranite, granodiorite, tonalite and pegmatite; alternating biotite- and feldspar-rich layers; includes layers and lenses of amphibolite and ultramafic schist.|
37550|Golden Eagle Orthogneiss|66118|5|Briefly described|p147|||Pilbara Craton. Kurrana Terrane.|3178+/-3 Ma, Nelson 2003|||||
37550|Golden Eagle Orthogneiss|69167|4|Described|geologyp_lut.csv|Mesoarchean|Paleoarchean|Age derived from samples of foliated tonalite gneiss and quartz diorite gneiss(178012.1.pdf, 178013.1.pdf) and is the age of crystalization of the protoliths to the gneisses|3178 +/- 3 Ma - 3225 +/- 5 Ma(SHRIMP)|Mount Billroth Supersuite|||Layered orthogneiss derived from tonalite, granodiorite, monzogranite, and pegmatite; includes layers and lenses of amphibolite and ultramafic schist.|
37550|Golden Eagle Orthogneiss|69590|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Paleoarchean|Geological province: Kurrana Terrane, Pilbara Craton, West Australian Craton. Events: Split Rock Supersuite Event; Mosquito Creek Orogeny; East Pilbara Terrane Rifting Event. Sample GSWA 178012 (biotite tonalite gneiss) yielded an interpreted crystallisation age of either 3150+\-9 Ma or 3178+\-3 Ma for the tonalite. If the c. 3150 Ma represents crystallisation age, then c. 3178 Ma age would indicate zircon xenocrysts. If c. 3178 Ma represents crystallisation age, then c. 3150 Ma represents Pb loss. Sample GSWA 178013 (quartz diorite gneiss) yielded an interpreted crystallisation age of 3225+\-5 Ma for the dioritic precursor to the gneiss. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3199-3178 Ma (isotopic)|Unit of Mount Billroth Supersuite.||Locally interleaved with Coondamar Formation.|Layered orthogneiss derived from tonalite, granodiorite, monzogranite, and pegmatite; includes layers and lenses of amphibolite and ultramafic schist|
37550|Golden Eagle Orthogneiss|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||felsic gneiss, syenogranite, monzogranite|
37550|Golden Eagle Orthogneiss|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||Max age 3199+/-3 Ma, min 3178+/-3 Ma.|Mount Billroth Supersuite|||Layered orthogneiss derived from tonalite, granodiorite, monzogranite, and pegmatite; includes layers and lenses of amphibolite and ultramafic schist.|
37550|Golden Eagle Orthogneiss|72668|5|Briefly described|p11, p15|||Kurrana Terrane. Intrudes undated greenstones.|c. 3200-3180 Ma|Mount Billroth Supersuite||||
80116|Golden Empress Gabbro|71212|4|Described|intro p2, p60, p46, p59|||Yilgarn Craton. One of 5 informal units that are together equivalent to the formal Bounty Igneous Complex. Up to 500m thick. See also  p52, 53, p89, p199, p216, p218.||||Intrudes the Never Can Tell Basalt.|Massive, medium and even-grained gabbro that is sporadically pyroxene-phyric.|26-SEP-17
78987|Golden Grove Member|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton.|c.2963 Ma.|Gossan Hill Formation.|||Rhyodacite, rhyolite and laminated felsic volcaniclastic rocks; host to economic massive sulfide horizons; metamorphosed.|
78987|Golden Grove Member|70796|5|Briefly described|100k_geologyp_lut.csv|Mesoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. See also 100K_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 203702.1.pdf, 203703.1.pdf, 203703.1.pdf, 203704.1.pdf, Badja100_2240_stratig.pdf. Numerous additional lithologies are discussed.|2963 +/ 6 Ma (isotopic)|Gossan Hill Formation||Overlain by the Scuddles Member.|Rhyodacite, rhyolite and laminated felsic volcaniclastic rocks; host to economic massive sulphide horizons; metamorphosed|
78987|Golden Grove Member|71269|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). Sample GSWA 203703 (metarhyolite) yielded a weighted mean 207Pb/206Pb date of 2963+\-6 Ma, interpreted as the magmatic crystallization age of the rhyolite protolith. Sample GSWA 203704 (metarhyolite) yielded a weighted mean 207Pb/206Pb date of 2959+\-5 Ma, interpreted as the magmatic crystallization age of the rhyolite protolith. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv.|2963+\-5 Ma (isotopic)|Unit of Gossan Hill Formation.||Overlain by Scuddles Member.|Rhyodacite, rhyolite and laminated felsic volcaniclastic rocks; host to economic massive sulphide horizons; metamorphosed|
78987|Golden Grove Member|71272|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c.2963 Ma.|Gossan Hill Formation.|||Rhyodacite, rhyolite and laminated felsic volcaniclastic rocks; host to economic massive sulfide horizons; metamorphosed.|
26586|Golden Mile Dolerite|22534|6|Mentioned|Fig.5 p10|||of Black Flag Group||||||
26586|Golden Mile Dolerite|22596|5|Briefly described|p413, Fig.5 p416|Archean|Archean|||||||07-NOV-08
26586|Golden Mile Dolerite|23137|5|Briefly described|p246|||||||||
26586|Golden Mile Dolerite|23149|5|Briefly described|p101|||||||||
26586|Golden Mile Dolerite|23159|6|Mentioned|p805|Archean|Archean|||||||07-NOV-08
26586|Golden Mile Dolerite|23786|6|Mentioned|p7|||Geological Province: Yilgarn Craton.||||||
26586|Golden Mile Dolerite|23853|5|Briefly described|p834|||||||||
26586|Golden Mile Dolerite|23924|5|Briefly described|p206|Archean|Archean|Geological Province: Yilgarn Craton.  Age: 2675 +/- 4 Ma (U-Pb).||||||07-NOV-08
26586|Golden Mile Dolerite|23926|6|Mentioned|p10 Tb. 1|||||||||
26586|Golden Mile Dolerite|23928|5|Briefly described|p66|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
26586|Golden Mile Dolerite|24306|5|Briefly described|p943|||||||||
26586|Golden Mile Dolerite|29681|5|Briefly described|Table 2|||||||||
26586|Golden Mile Dolerite|29784|6|Mentioned|Table 1|||||||||
26586|Golden Mile Dolerite|30567|6|Mentioned|p415|||||||||
26586|Golden Mile Dolerite|30779|4|Described|p21|||Also mention Fig.2||||||
26586|Golden Mile Dolerite|30882|6|Mentioned|p50|||||||||
26586|Golden Mile Dolerite|30886|5|Briefly described|p19|||Also mention Table 4.||||||
26586|Golden Mile Dolerite|30900|6|Mentioned|p67|||See also Table 1||||||
26586|Golden Mile Dolerite|31042|6|Mentioned|Fig. 4|||Correlation||||||
26586|Golden Mile Dolerite|32078|6|Mentioned|p248|||||||||
26586|Golden Mile Dolerite|32079|6|Mentioned|p435|||||||||
26586|Golden Mile Dolerite|32083|5|Briefly described|p294|||||||||
26586|Golden Mile Dolerite|32447|6|Mentioned|p9|||||||||
26586|Golden Mile Dolerite|32685|5|Briefly described|Table 1|||||||||
26586|Golden Mile Dolerite|33513|4|Described|p29|||See also p27. Main ore host||||||06-MAY-21
26586|Golden Mile Dolerite|33514|6|Mentioned|p19|||||||||
26586|Golden Mile Dolerite|33515|6|Mentioned|p33|||||||||
26586|Golden Mile Dolerite|33535|4|Described|p184|||See also P185||||||
26586|Golden Mile Dolerite|33554|6|Mentioned|p72|||||||||
26586|Golden Mile Dolerite|33838|6|Mentioned|p68|||||||||
26586|Golden Mile Dolerite|33917|5|Briefly described|p177|||lithology||||||
26586|Golden Mile Dolerite|34281|6|Mentioned|p14|||||||||
26586|Golden Mile Dolerite|34324|6|Mentioned|p122|||||||||
26586|Golden Mile Dolerite|34608|6|Mentioned|p2|||||||||
26586|Golden Mile Dolerite|35469|6|Mentioned|p44|||||||||
26586|Golden Mile Dolerite|35611|6|Mentioned|Fig.2|||Stratigraphic columns for Kalgoorlie and Kambalda.||||||
26586|Golden Mile Dolerite|35612|5|Briefly described|p4|||Discussed re Kalgoorlie gold deposits||||||
26586|Golden Mile Dolerite|36259|5|Briefly described|p63|||Overlies Paringa Basalt; overlain by Black Flag Beds. Complex differentiated intrusion comprising up to 10 conformable units, ranging in composition from a lower ultramafic chilled contact to a quartz-rich, granophyric in the upper section.||||||12-MAR-08
26586|Golden Mile Dolerite|36869|5|Briefly described|p40|||See also P48||||||
26586|Golden Mile Dolerite|38765|6|Mentioned|p100|||||||||
26586|Golden Mile Dolerite|39046|5|Briefly described|p438|||||||||
26586|Golden Mile Dolerite|39895|4|Described|p55|||||||||
26586|Golden Mile Dolerite|40005|6|Mentioned|Fig.3|||||||||
26586|Golden Mile Dolerite|40083|6|Mentioned|Fig.2|||||||||
26586|Golden Mile Dolerite|40799|6|Mentioned|p246|||||||||
26586|Golden Mile Dolerite|40845|4|Described|p81|||||||||
26586|Golden Mile Dolerite|40849|6|Mentioned|p37|||||||||
26586|Golden Mile Dolerite|41066|5|Briefly described|2 of 2 C01|||Mention P34||||||
26586|Golden Mile Dolerite|41096|6|Mentioned|p301|||||||||
26586|Golden Mile Dolerite|41149|5|Briefly described|p1664|||||||||
26586|Golden Mile Dolerite|41249|4|Described|p22|||||||||
26586|Golden Mile Dolerite|41379|6|Mentioned|p39|||||||||
26586|Golden Mile Dolerite|41458|6|Mentioned|p361|||||||||
26586|Golden Mile Dolerite|41673|6|Mentioned|p9|||||||||
26586|Golden Mile Dolerite|41771|6|Mentioned|Fig.3|||||||||
26586|Golden Mile Dolerite|41784|6|Mentioned|p65|||||||||
26586|Golden Mile Dolerite|41889|5|Briefly described|p218|||||||||
26586|Golden Mile Dolerite|41900|6|Mentioned|p134|||||||||
26586|Golden Mile Dolerite|42117|5|Briefly described|Table 1 P67|||||||||
26586|Golden Mile Dolerite|42195|5|Briefly described|p146|||See also Fig.4||||||
26586|Golden Mile Dolerite|42198|6|Mentioned|p262|||||||||
26586|Golden Mile Dolerite|42221|5|Briefly described|p10|||||||||
26586|Golden Mile Dolerite|42344|6|Mentioned|p52|||||||||
26586|Golden Mile Dolerite|42436|6|Mentioned|Fig.11 P.84|||||||||
26586|Golden Mile Dolerite|42570|5|Briefly described|p661|||||||||
26586|Golden Mile Dolerite|42696|6|Mentioned|Plate 1B|Archean||||||||07-NOV-08
26586|Golden Mile Dolerite|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
26586|Golden Mile Dolerite|42817|5|Briefly described|Fig.3|||||||||
26586|Golden Mile Dolerite|42870|5|Briefly described|Table 1, P67|||||||||
26586|Golden Mile Dolerite|42892|6|Mentioned|p36|||||||||
26586|Golden Mile Dolerite|42969|6|Mentioned|Fig.1 p106|||||||||
26586|Golden Mile Dolerite|43102|5|Briefly described|Fig.2|||||||||
26586|Golden Mile Dolerite|43162|6|Mentioned|5|||||||||
26586|Golden Mile Dolerite|43496|4|Described|6-15|||Age: 2675+/-6Ma.||||||03-MAR-10
26586|Golden Mile Dolerite|43735|6|Mentioned|p44|||||||||
26586|Golden Mile Dolerite|44149|6|Mentioned|p88 fig 2-90|Archean|Archean|||||||
26586|Golden Mile Dolerite|45546|14|Not recorded|p.50-52|||"The principle orebodies are located in quartz dolerites of the Golden Mile Dolerite".||||||
26586|Golden Mile Dolerite|46905|5|Briefly described|Table 1|||Stratigraphic succession||||||
26586|Golden Mile Dolerite|50622|4|Described|p314|||Thickness: 600-940m.  Can be divided into 10 informal units. Intruded contacts between Paringa Basalt and Black Flag Beds.||||||24-NOV-04
26586|Golden Mile Dolerite|60076|5|Briefly described|p22|Archean|Archean|A differentiated (micro-) gabbroic sill, the main host to Kalgoorlie-Boulder gold mineralisation.||||||07-NOV-08
26586|Golden Mile Dolerite|60514|6|Mentioned|p30, p54|Archean|Archean|Maximum thickness: 700m. Gabbro sill. Geological Province: Yilgarn Carton.||||||07-FEB-11
26586|Golden Mile Dolerite|60623|6|Mentioned|p30|Archean|Archean|||||||07-NOV-08
26586|Golden Mile Dolerite|60626|4|Described|p54|||Thickness: 700 m. Subdivided into 10 units. Equivalent to Aberdare Dolerite.||||||
26586|Golden Mile Dolerite|60627|5|Briefly described|p65 Tb.1|||Intrudes Black Flag Group||||||
26586|Golden Mile Dolerite|60976|6|Mentioned|p16|||Geological Province: Yilgarn Craton.||||||
26586|Golden Mile Dolerite|60981|6|Mentioned|p187 Fig.6|||||||||
26586|Golden Mile Dolerite|61855|5|Briefly described|p333, p334|||Covered by nodular and pisolitic gravels with massive lateritic duricrusts.||||||
26586|Golden Mile Dolerite|62108|5|Briefly described|p1409 Tb. 1|||Differentiated into 10 units. Geological Province: Yilgarn Craton (Boulder-Lefroy Shear Zone). See also p1420 Fig.14.||||||07-FEB-11
26586|Golden Mile Dolerite|62109|5|Briefly described|p1428, p1429 Fig. 2|||Rhyolite porphyry dykes; parts are described as amphibolitic and others chloritic (see Fig. 2). The prinicipal host rock to lode structures in Kalgoorlie. Intrude the lower Black Flag Group. Thickness: 750m.||||||14-APR-08
26586|Golden Mile Dolerite|62406|6|Mentioned|p55|||||||||
26586|Golden Mile Dolerite|62872|5|Briefly described|p805|||Igneous intrusion. Discusses Golden Mile mineralisation located at southern end of Kalgoorlie gold field.||||||
26586|Golden Mile Dolerite|63163|5|Briefly described|p76|||Overlain by Black Flag Group; underlain by Paringa Basalt. Max. thickness: 700m. Geological Province: Kalgoorlie Terrane/Eastern Goldfields Province. Layered tholeiitic sill.||||||
26586|Golden Mile Dolerite|63981|6|Mentioned|p95 Fig.5, p97|Archean|Archean|In LED-10, intrudes the contact between Paringa Basalt and Kalgoorlie Sequence. Its upper surface is hydraulically-brecciated contact aureole; interpreted emplacement depth of at least 5 km.||||Intrudes Kalgoorlie Sequence.|Gabbro.|
26586|Golden Mile Dolerite|64715|5|Briefly described|p3, p5 Fig. 4|||Main host rocks for Kalgoorlie gold deposits. See also p7 Fig. 7.||||||16-DEC-08
26586|Golden Mile Dolerite|65204|5|Briefly described|pg6 Tbl.1, p12, p24|Archean|Archean|A differentiated gabbroic sill; the main host to gold mineralisation on the Golden Mile, also hosts the Mount Charlotte deposit; associated with smaller sills including Williamstown Dolerite.||||||
26586|Golden Mile Dolerite|65264|5|Briefly described|p22|||Comprises a differentiated (micro-)gabbroic sill that is the main host to gold mineralisation at Kalgoorlie-Boulder.||||||07-FEB-11
26586|Golden Mile Dolerite|65834|6|Mentioned|p7, 12, 53-58|||Kambalda Domain, Kalgoorlie Terrane. Subdivided into ten units showing a tholeiitic differentiation trend. Hosts gold mineralisation (eg Mount Charlotte orebody).||Black Flag Group.||||
26586|Golden Mile Dolerite|68109|6|Mentioned|p660|||Kalgoorlie Terrane.|||||Auriferous; mafic sills.|
26586|Golden Mile Dolerite|68216|6|Mentioned|p301 Fig. 1|||SH51-9||||||
26586|Golden Mile Dolerite|68217|4|Described|p71-79|Precambrian|Precambrian|Approx 1000-2500 ft thick [~300-763m thick]||||Underlain by Paringa Basalt. Overlain by Black Flag Beds.|Sill of meta-quartz dolerite and meta-quartz gabbro with minor more basic sections|
26586|Golden Mile Dolerite|68289|6|Mentioned|p12-p13|||Mount Hunt-Hannan Lake area.||||||
26586|Golden Mile Dolerite|69035|5|Briefly described|pp411-418, pp423-424, pp427-430|Neoarchean|Neoarchean|~ 600 to 940 m thick. Tholeiitic sill occupying consistent stratigraphic position over ~ 20 km strike, locally discordant with bedding in the Black Flag Beds. Subdivided into ten sub-units by Travis, Woodall and Bartram (1971).|2660 +/- 100 Ma, Rb-Sr (Turek 1966)||||Weakly differentiated gabbroic sill, with upper and lower chilled margins, a lower ultramafic layer, several gabbroic units, an iron-rich microgabbro, and a central granophyric unit.|
26586|Golden Mile Dolerite|69404|6|Mentioned|p4|||Kalgoorlie Terrane. Economically important.||Black Flag Group||||
26586|Golden Mile Dolerite|69619|6|Mentioned|p115|||||||Intrudes Kalgoorlie Sequence.|Differentiated dolerite.|
26586|Golden Mile Dolerite|69631|6|Mentioned|p14, p16|||||||||
26586|Golden Mile Dolerite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2680 +/- 9 Ma (isotopic).|Great Boulder Suite|||Differentiated gabbroic sill; cumulate pyroxenite to granophyre; metamorphosed.|
26586|Golden Mile Dolerite|70287|6|Mentioned|p187-196, 210, 213|||Kalgoorlie Gold Field. A dolerite sill. May have undergone late gold mineralisation or remobilisation between ~2.61 and 2.60 Ga. Intruded along the Paringa Basalt/Kalgoorlie Sequence contact.|2680 +/- 9 Ma (Rasmussen et al., 2009).||||Tholeiitic; Fe-rich; ten mappable units.|
26586|Golden Mile Dolerite|70290|5|Briefly described|p295-299, 301, 303-304, 306|||Kalgoorlie, Eastern Goldfields Province, Yilgarn Craton. The main host to gold in the Kalgoorlie deposits. Presented as GMD for much of the article. 600-750m thick; extends 13km along strike. Subdivided into ten petrographic units. Mineralisation occurred at 2642 +/- 6 Ma. Trace element composition tabulated. Photographs, photomicrographs.|2680 +/- 9 Ma (Pb-Pb; Rasmussen et al., 2009).||||An auriferous tholeiitic dolerite sill. Metamorphosed to an actinolite-albite-epidote assemblage replaced by hydrothermal chlorite and calcite.|
26586|Golden Mile Dolerite|70326|5|Briefly described|p360|Neoarchean|Neoarchean|Geological province: Kalgoorlie Domain, Kalgoorlie Terrane, Yilgarn Craton. Age from granophyre, U-Pbzirconolite and xenotime SHRIMP (Rasmussen et al., 2009).|2680+\-9 Ma (Rasmussen et al., 2009).|||Intrudes into lower Black Flag Group. Correlable to Condensor Dolerite.||
26586|Golden Mile Dolerite|70773|6|Mentioned|p24 fig 16, p25 fig 18|||||||||
26586|Golden Mile Dolerite|71148|6|Mentioned|p18|Neoarchean|Neoarchean||c.2694 Ma.|||||
26586|Golden Mile Dolerite|71166|5|Briefly described|p35, p118, p119 fig 3.89|||At Mount Charlotte gold ore is confined to this unit. Gold mineralization also occurs at the Fimiston Superpit where it is associated with iron-rich zones. SHRIMP U-Pb date derived from Rasmussen et al, 2009. |2680 +/- 9 Ma (SHRIMP U-Pb)||||Iron rich dolerite.|
26586|Golden Mile Dolerite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2680+\-9 Ma|Unit of Great Boulder Suite.|||Differentiated gabbroic sill; cumulate pyroxenite to granophyre; metamorphosed|
26586|Golden Mile Dolerite|71308|5|Briefly described|p729|||Has distinst affinities with the authors' Low-Th Basalt group.|2680 +/- 9 Ma.|||Intrudes Black Flag Beds.|Mafic sills.|
26586|Golden Mile Dolerite|72049|4|Described|p251, p257-p259, p268, p272|||Kalgoorlie and Kurnalpi terranes. SHRIMP age is derived from Rasmussen et al., 2009.|2680 +/- 9 Ma (SHRIMP U-Pb)|||Intrudes the Black Flag Group.|Dolerite.|
26586|Golden Mile Dolerite|72057|4|Described|p236,238-240,243-245,247-249|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton. Contact with Black Flag Group host sediments is irregular, indicating emplacement into unconsolidated sediments and at relatively shallow depths. Interpreted as an intrusive sill, based on common coarse (>3mm) groundmass grain size, thin hosting sediments indicating relatively flat paleo-depositional enviroment (thus not conducive for lava ponding) and extensive sheet-like geometry. Comprises large (~75-460m thick, up to 750m, over tens of kms long) medium to coarsely crystalline mafic rocks, including a variety of products of differentiation; emplaced in mudstones and basalt and concordant to stratigraphy. U-Pb crystallisation age, based on magmatic zircons from the granophyre, is 2675+\-2 Ma (Woods, 1997). Metamorphosed to greenschist facies.|c. 2680 Ma|Unit of Black Flag Group.|||Gabbro, quartz gabbro, basalt, lesser dolerite.|
26586|Golden Mile Dolerite|72095|4|Described|p10-11, 14-17,20-21|||Kalgoorlie Region, Eastern Goldfields, Yilgarn Craton. Detailed geochemistry is described. Geochemically very similar to Lunnon Basalt, Condensor Dolerite when only TiO2 vs Th, Nb, Zr, La considered.||||Similar stratigraphic level as Eureka Dolerite.||10-MAY-23
26586|Golden Mile Dolerite|73300|6|Mentioned|p1112-1113, p1118 Fig.7|Neoarchean|Neoarchean|Yilgarn Craton, Kalgoorlie terrane. Primary host rock to gold mineralisation in the Kalgoorlie gold camp.|2685 +/- 4 Ma||||Dolerite sill, intrudes volcano-sedimentary sequence.|
26586|Golden Mile Dolerite|73391|5|Briefly described|vii, 26, 109, 111-115, 133, 181, 186|||See also p194, 197, 200, 204, 230, 232, 240, 244, 303-304, 308-309, 347, 442, Appendices. Kambalda Domain, Kalgoorlie Terrane. Hosts the largest (70 million ounces) Archaean greenstone gold deposit in the north Kalgoorlie district. Also dated at 2675 +/- 3 Ma (SHRIMP).|2685 +/- 4 Ma (SHRIMP: Tripp, 2019).|||Is overlain by Lakewood dacite volcanics, Talbot formation. Intrudes base of Spargoville Formation at contact with underlying Paringa Basalt.|Layered basic sill: sericite-chlorite-carbonate-magnetite altered granophyric quartz-dolerite sill.|
26586|Golden Mile Dolerite|73596|6|Mentioned|p1161|Neoarchean|Neoarchean|Kalgoorlie area.|2680 +/- 9 Ma.|||Intrudes Black Flag Group. Correlated with Mount White Dolerite.||
35674|Golden Valley Conglomerate|23142|5|Briefly described|p203 Fig.2|||||||||
35674|Golden Valley Conglomerate|60514|6|Mentioned|p48 Fig. 2|Archean|Archean|Rounded mafic rudite. Geological Province: Yilgarn Craton.||||||07-FEB-11
35674|Golden Valley Conglomerate|60625|5|Briefly described|p48 Figs. 1, 2|||Rounded mafic rudite. Geological Province: Eastern Goldfields.||||||
35674|Golden Valley Conglomerate|65834|6|Mentioned|p36|||Kanowna Belle gold mine, Boorara Domain, Kalgoorlie Terrane. Mine terminology.||||Is intruded by Kanowna Belle Porphyry.|Mafic-rich conglomerate.|
35674|Golden Valley Conglomerate|70482|5|Briefly described|p319, 323-324|Archean|Archean|Part of greenstone successions around the Scotia-Kanowna Dome, Eastern Goldfields Superterrane, Eastern Yilgarn Craton. Over 400m thick. Located N of the Fitzroy Fault.|2668 +/- 9 Ma (MDA: Tripp et al., 2007).|Kalgoorlie Sequence.||Is overlain conformably by Golden Valley turbidite.|Poorly sorted, internally massive to weakly graded beds; dominated by porphyritic and equigranular felsic clasts with minor mafic and volcaniclastic clasts.|
35674|Golden Valley Conglomerate|72049|5|Briefly described|p256, p259, p270|||Geochronology analyses, results, and interpretation are discussed in detail.||Late Merougil Group.||||18-MAR-19
35674|Golden Valley Conglomerate|73391|5|Briefly described|p26, 51, 161-163, 165-166, 189-191|Neoarchean|Neoarchean|See also p199, 224, 241, 304, 413, Appendix p110. Kanowna district. Also appears as Golden Valley conglomerate. Almost certainly not intended as a formal unit, despite the capitalisation. Both names used interchangeably with Golden Valley member (see references p132, 148, 159-166, 174, 182-183, 189, 194, 196, 224, 244, 247, 444). Total thickness ~1800m, but probably more.|2668 +/- 9 Ma (MDA: Ross et al., 2004).|||Overlies Government Dam Turbidite.|An E-dipping sequence comprising basal conglomerate, then grit, siltstone and turbidite.|22-JUN-22
25928|Goldwyer Formation|7433|6|Mentioned|p25 Fig.2, p28 Fig.5, p29.|Ordovician|Ordovician|Canning Basin. Fine clastics; marine.||||||
25928|Goldwyer Formation|12891|6|Mentioned|p734|Llanvirnian|Late Arenigian|Geological province: Canning Basin.||||||07-FEB-11
25928|Goldwyer Formation|13255|6|Mentioned|p368|Middle Ordovician|Middle Ordovician|Roebuck Basin.||||Overlies Willara Formation. Is overlain by Nita Formation.||
25928|Goldwyer Formation|13995|5|Briefly described|p67-68, p83, p87, p101|Ordovician|Ordovician|Canning Basin. Six of the twelve species of chitinozoans in this unit occur in coeval assemblages in Spitsbergen and Laurentia. Has a rich trilobite fauna (listed), in association with graptolites. Has mixed conodont assemblages. Darriwilian.||||Conformably or disconformably overlies Willara Formation. Is overlain by Nita Formation.|Dark, thin-bedded, graptolitic calcareous shales and thin limestones.|
25928|Goldwyer Formation|14228|5|Briefly described|p6 fig3|Middle Ordovician|Middle Ordovician|Canning Basin.||||Overlies Willara Formation. Overlain by Nita Formation.||05-OCT-16
25928|Goldwyer Formation|22646|6|Mentioned|p 106|Early Ordovician|Early Ordovician|Canning Basin||||||
25928|Goldwyer Formation|22738|6|Mentioned|5|Ordovician|Ordovician|Max thickness 750 m. Overlying units Grant Group, Nita Formation, underlying unit Willara Formation||||||
25928|Goldwyer Formation|22741|6|Mentioned|P21|||||||||
25928|Goldwyer Formation|22753|5|Briefly described|Fig.3 p585|Ordovician|Ordovician|||||||
25928|Goldwyer Formation|22764|6|Mentioned|p13||Early Ordovician|WAPET Barbwire No. 1 well||||||01-FEB-10
25928|Goldwyer Formation|22765|5|Briefly described|P7, Table1|Llanvirn|Arenig|||||||
25928|Goldwyer Formation|22767|5|Briefly described|Table3 P18, P11||Ordovician|||||||
25928|Goldwyer Formation|22776|4|Described|p10, Table.3|Ordovician|Ordovician|||||||
25928|Goldwyer Formation|22801|5|Briefly described|P10, Table1 P9||Ordovician|||||||
25928|Goldwyer Formation|22814|5|Briefly described|fig2|Ordovician|Ordovician|||||||
25928|Goldwyer Formation|22823|6|Mentioned|p514|||Geological Province - Canning Basin.||||||
25928|Goldwyer Formation|23212|4|Described|Table.1 p6||Ordovician|Age: Middle Ordovician.||||||
25928|Goldwyer Formation|23356|5|Briefly described|26 Tab.2|Ordovician|Ordovician|||||||
25928|Goldwyer Formation|23534|5|Briefly described|p2322||Ordovician|||||||
25928|Goldwyer Formation|24061|4|Described|p177|Middle Ordovician|Early Ordovician|Geological Province:  Canning Basin. Maximum thickness: 737m.||||||
25928|Goldwyer Formation|24062|5|Briefly described|p186 Table 1|Ordovician|Ordovician|Geological Province: Canning Basin.||||||
25928|Goldwyer Formation|24246|5|Briefly described|p11|||Geological Province: Canning Basin.||||||
25928|Goldwyer Formation|24390|5|Briefly described|p6 Fig. 4|Ordovician|Ordovician|Geological Province: Canning Basin.||||||
25928|Goldwyer Formation|24449|5|Briefly described|p744, p741 Fig. 2|Llanvirnian|Llanvirnian|Geological Province: Canning Basin.  See also p473 Fig. 5.||||||
25928|Goldwyer Formation|29813|6|Mentioned|p16|||||||||
25928|Goldwyer Formation|30110|6|Mentioned|p81|||See also P82. Llanvirnian age.||||||
25928|Goldwyer Formation|30313|4|Described|p54|||Middle to Upper Ordovician||||||
25928|Goldwyer Formation|30595|5|Briefly described|p3|||||||||
25928|Goldwyer Formation|32648|6|Mentioned|p32|||M. Ord.||||||
25928|Goldwyer Formation|33518|6|Mentioned|p4|||||||||
25928|Goldwyer Formation|33738|6|Mentioned|p55|||||||||
25928|Goldwyer Formation|33965|4|Described|Table 1|||||||||
25928|Goldwyer Formation|35119|4|Described|p462|||Mention Text-Fig.3.||||||
25928|Goldwyer Formation|35127|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
25928|Goldwyer Formation|35201|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
25928|Goldwyer Formation|35222|4|Described|Table.2|||||||||
25928|Goldwyer Formation|35223|4|Described|Table.2|||||||||
25928|Goldwyer Formation|35250|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
25928|Goldwyer Formation|35251|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
25928|Goldwyer Formation|35275|6|Mentioned|Fig.5.|||||||||
25928|Goldwyer Formation|35497|4|Described|Table 1|||Also on p7.||||||13-NOV-07
25928|Goldwyer Formation|35903|4|Described|Table 1|||||||||
25928|Goldwyer Formation|36224|5|Briefly described|Map legend|Ordovician|Ordovician|Siltstone, sandstone, shale; minor dolomite, limestone.  Conformably overlain by Nita Formation.||||||01-FEB-05
25928|Goldwyer Formation|36257|6|Mentioned|Table 2.1|||||||||
25928|Goldwyer Formation|36438|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
25928|Goldwyer Formation|36634|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
25928|Goldwyer Formation|36890|3|Fully described|p324|||||||||
25928|Goldwyer Formation|37368|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
25928|Goldwyer Formation|37369|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
25928|Goldwyer Formation|37370|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
25928|Goldwyer Formation|38878|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
25928|Goldwyer Formation|39854|6|Mentioned|p21|||||||||
25928|Goldwyer Formation|39857|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
25928|Goldwyer Formation|40078|6|Mentioned|Map legend|Middle Ordovician|Early Ordovician|Early to Middle OrdovicianE - M||||||
25928|Goldwyer Formation|40136|5|Briefly described|p26|||||||||
25928|Goldwyer Formation|40837|6|Mentioned|p271|||||||||
25928|Goldwyer Formation|40992|6|Mentioned|Fig.11|||||||||
25928|Goldwyer Formation|41169|6|Mentioned|p140|||||||||
25928|Goldwyer Formation|41209|4|Described|p143|||||||||
25928|Goldwyer Formation|41215|6|Mentioned|p267|||||||||
25928|Goldwyer Formation|41436|6|Mentioned|p44|||||||||
25928|Goldwyer Formation|41583|6|Mentioned|p22|||||||||
25928|Goldwyer Formation|41730|6|Mentioned|p472|||||||||
25928|Goldwyer Formation|41854|4|Described|p94|||||||||
25928|Goldwyer Formation|41913|6|Mentioned|Fig.2 P107|||||||||
25928|Goldwyer Formation|42058|6|Mentioned|p123|||||||||
25928|Goldwyer Formation|42347|6|Mentioned|Fig.2 P1020|||||||||
25928|Goldwyer Formation|42880|5|Briefly described|Fig.2,p1020|||||||||
25928|Goldwyer Formation|42930|5|Briefly described|Fig.1 p473|Ordovician|Ordovician|Overlies and interfingers with Willara Formation; conformably underlies Nita Formation. Geological Province: Canning Basin.||||||13-NOV-07
25928|Goldwyer Formation|43117|5|Briefly described|Table 1,p349|||||||||
25928|Goldwyer Formation|43173|6|Mentioned|11-54||Ordovician|||||||
25928|Goldwyer Formation|43236|6|Mentioned|p14||Ordovician|Canning Basin||||||
25928|Goldwyer Formation|43563|6|Mentioned|p4|||||||||
25928|Goldwyer Formation|43599|6|Mentioned|p250, Fig.3||Llanvirnian|||||||
25928|Goldwyer Formation|43656|6|Mentioned|Fig.2,p8|Llanvirnian|Llanvirnian|||||||
25928|Goldwyer Formation|43666|6|Mentioned|p19|Llanvirnian|Arenigian|||||||
25928|Goldwyer Formation|43746|6|Mentioned|Fig.2,p11|Llanvirnian|Llanvirnian|||||||
25928|Goldwyer Formation|43803|6|Mentioned|p65||Ordovician|||||||
25928|Goldwyer Formation|43815|6|Mentioned|Table 2,p95-96|||||||||
25928|Goldwyer Formation|43818|6|Mentioned|Fig.2.p39||Early Ordovician|||||||
25928|Goldwyer Formation|43825|5|Briefly described|p143||Ordovician|Hydrocarbon source rock. Barbwire Terrace.||||||
25928|Goldwyer Formation|44143|4|Described|p426, p428, p441 Table 4-19|Ordovician|Ordovician|Up to 736m thick; shale, limestone & dolomite; shallow marine. Conformably overlies Willara Formation and Wilson Cliffs Sandstone. Contains trilobites, graptolites, brachiopods, conodonts & ostracods; Llanvirnian. Type section between 848m and 1060 m in Thangoo 1A (LAGRANGE: 18 deg 21' 52" S, 122 deg 53' 09" S). Has petroleum source-rock potential.||||||
25928|Goldwyer Formation|44356|6|Mentioned|p8||Early Ordovician|(Middle Ordovician)||||||
25928|Goldwyer Formation|44357|5|Briefly described|p11,Tb.1 p10||Early Ordovician|(Middle Ordovician)||||||
25928|Goldwyer Formation|45153|2|Defined|App.1-7|Llanvirnian|Llanvirnian|||||||
25928|Goldwyer Formation|45158|3|Fully described|p28|||||||||
25928|Goldwyer Formation|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
25928|Goldwyer Formation|50085|5|Briefly described|p6 Fig. 4|Ordovician|Ordovician|Geological Province: Canning Basin.||||||
25928|Goldwyer Formation|50089|5|Briefly described|p430 Fig. 5|Ordovician|Ordovician|Geological Province: Canning Basin.||||||
25928|Goldwyer Formation|50091|5|Briefly described|p413 Tb. 1|Middle Ordovician|Middle Ordovician|Occurrence of Panderodus nogamii (conodonts).  Geological Province: Canning Basin.||||||04-NOV-04
25928|Goldwyer Formation|61020|6|Mentioned|p33 Fig. 4|||Lead for petroleum potential.  Geological Province: Canning Basin.||||||20-APR-05
25928|Goldwyer Formation|61021|5|Briefly described|p36 Fig. 2|Llanvirnian|Llanvirnian|Overlain by the Nita Formation. Geological Province: Canning Basin.||||||17-DEC-07
25928|Goldwyer Formation|61023|5|Briefly described|p10 Fig. 6|Middle Ordovician|Middle Ordovician|Mudstone and carbonate package. Age is Llanvirnian. Geological Province: Canning Basin. See also p11.||||||11-APR-08
25928|Goldwyer Formation|61551|5|Briefly described|p351 Fig.2, p352, p355, p359. |Darriwilian|Darriwilian|Onshore Canning Basin. Hydrocarbon source rocks; sealed by the Carribuddy Group. Conodonts range from upper Histiodella holodentata Zone to the lower Phragmodus-Plectodina Zone, indicating an early Llanvirn age (Nicoll, 1993; Nicoll et al, 1993). |~470-465 Ma (2004 timescale).|||Overlies Willara Formation.||03-SEP-18
25928|Goldwyer Formation|62794|6|Mentioned|p298|Early Ordovician|Early Ordovician|Canning Basin. Contains trilobites.||||||
25928|Goldwyer Formation|62982|5|Briefly described|p7|Ordovician|Ordovician|Bioturbated carbonate and mudstone deposits; richly fossiliferous. Carbonate reefs developed during deposition. Overlies Willara  Formation; overlain by Nita Formation. Geological Province: Canning Basin.||||||16-JAN-07
25928|Goldwyer Formation|64015|6|Mentioned|p72|||Geological province:Canning Basin.||||||28-AUG-08
25928|Goldwyer Formation|64185|5|Briefly described|p158 Fig. 2, p163|Early Ordovician|Early Ordovician|Underlain conformably by Willara Formation, overlain conformably by Nita Formation. Marine.||||||
25928|Goldwyer Formation|64186|4|Described|p169, p171, p177|Ordovician|Ordovician|Underlain by Willara Formation, usually conformable but a disconformity is indicated in one area. Overlain by Nita Formation. Max thickness: 212m. Black shale unit, generally with a middle limestone member.||||||
25928|Goldwyer Formation|64187|5|Briefly described|p320 Fig. 2|Middle Ordovician|Ordovician|Formation is Fm in text. Underlain unconformably by pre-Cambrian basement, overlain by Nita Formation. Carbonates, shales (marine). Geological Province: Canning Basin.||||||08-FEB-10
25928|Goldwyer Formation|64334|5|Briefly described|p39-43, 48|Ordovician|Ordovician|Canning Basin; subsurface only. Llanvirn. Regionally significant source rocks.||||Overlies Willara Formation, and locally Wilson Cliffs Sandstone unconformably. Is overlain by Nita Formation.|Mudstone, limestone. Fossiliferous.|
25928|Goldwyer Formation|64513|5|Briefly described|p23, p25, p26 Fig3, p28-29, p31, p33-35|Darriwilian|Darriwilian|Canning Basin. Unit description taken from lithologs diagram on p26 Fig3. Acritarchs described from 4 wells. Fauna indicates age range described as Llanvirn [equivalent to Darriwilian] .||||Conformably overlies Willara Formation and underlies Nita Formation.|Includes alternating layers of limestone, shale, claystone; minor dolostone towards the top.|
25928|Goldwyer Formation|64643|5|Briefly described|p3 Fig. 2|Darriwilian|Darriwilian|||||||
25928|Goldwyer Formation|64975|5|Briefly described|pp162-164.|Ordovician|Ordovician|Canning Basin. Contains well-developed hydrocarbon source horizons, with efficient Carribuddy evaporites seal.||||Is overlain by Nita Formation.|Interbedded fine-grained terrigenous clastics and carbonates.|
25928|Goldwyer Formation|64982|5|Briefly described|p699 Fig.4, pp701-702.|Llanvirn|Llanvirn|Excellent hydrocarbon source potential. Fossiliferous.||||Overlies Willara Formation. Is overlain by Nita Formation.|Interbedded shales and limestones, shoaling-upwards limestones and minor shales, shales with abundant Gloeocapsamorpha prisca algae.|
25928|Goldwyer Formation|65301|5|Briefly described|p3, p5 Fig. 4|Middle Ordovician|Middle Ordovician|Geological province: Canning Basin, Broome Platform. Dominated by marine shale and limestone. See also p8 Fig. 5.||||||
25928|Goldwyer Formation|65449|5|Briefly described|p3,p5-8,p11, p13-14, p37; Plates 1-11|Darriwilian|Darriwilian|Canning Basin. Fossiliferous marine unit. Appears also as Goldwire Formation on p13. Considered the most likely source of Ordovician shows in most parts of the Basin. See also Plates 7, 8, 9,10, 11.||||Overlies Willara Formation or Wilson Cliffs Sandstone. Is overlain by Nita Formation.||09-APR-20
25928|Goldwyer Formation|68007|4|Described|p1-2, p4-5, p11-15, Plates 1, 2|Middle Ordovician|Middle Ordovician|Canning Basin. Fossiliferous marine unit. About 253.5m thick in Patience 2 well. Oil and gas shows. An important regional source rock; in Kidson 1 well is described as overmature for oil generation; elsewhere it is considered early mature. TOC and rock eval pyrolysis data tabulated. Poor reservoir potential. Upper part is typified by abundant G.prisca algae. Composite well log.||||Overlies Wilson Cliffs Sandstone probably disconformably, and Willara Formation. Is overlain by Nita or Bongabinni Formations.|Interbedded black shales, limestone and, locally, very fine-grained sandstone. Occasional dolomite near the top.|
25928|Goldwyer Formation|68902|5|Briefly described|p6, p9 fig 5, p22-23|Ordovician|Ordovician |NW Canning Basin. Subsidence led to deposition of maximum flooding surface deposits. This Formation is well known for its potential source rock qualities. Forms a useful seismic reflector.||||Overlies Willara Formation, overlain by Nita Formation||
25928|Goldwyer Formation|69029|5|Briefly described|p313,315-316,319-320,333|Darriwilian|Darriwilian|Of Canning Basin. Avearage thickness: 400m. Thickest intersections includes 739m in Blackstone-1, Lennard Shelf and 736m from Willara-1 in the Willara Sub-basin. Mudstone-dominated in deeper basinal areas, and carbonate-dominated on platforms and terraces (Haines, 2004, 2009). Contains the richest source rocks in the Canning Basin. Organic-rich shales are oil-prone with TOC >5%. Source rocks are correlated to significant oil and gas discoveries in the Pictor and Dodonea areas. Previous shale-gas resources estimates include 229 Tcf (Kuuskra et al., 2001), and 61 bbl generative capacity on the Barbwire Terrace (Foster et al., 1986), and ~11bbl/km3 in the eastern Canning (Wulff, 1987). ||||Overlain by Bongabinni Formation. Underlain by Willara Formation.||
25928|Goldwyer Formation|69182|5|Briefly described|Ch4 p9-p12, Ch4 p20-p25|Middle Ordovician|Middle Ordovician|Canning Basin. May be more than 500m thick. Claystones within this formation are good potential seals for the storage of carbon dioxide. Poor prospectivity as a reservoir for carbon dioxide storage due to low average porosity. See also Ch4 p30-p36, Ch4 p39-p41, Ch4 p44-p45, Ch4 p47-p48, Ch4 p50-p58, Ch4 p62-p65, Ch4 p67, Ch4 p70, Ch4 p74, Ch4 p79-p82, Ch4 p92-p94. ||||Overlies the Willara Formation. Overlain by the Nita Formation.|Marl, shale, carbonates and claystones.|
25928|Goldwyer Formation|69206|6|Mentioned|p2-3|Ordovician|Ordovician|Canning Basin. Petroleum source.||||||
25928|Goldwyer Formation|69297|6|Mentioned|p350, p354|Early Ordovician|Early Ordovician|Canning Basin. Deposited under marine or supratidal conditions. Contains good potential oil source rocks. ||||||
25928|Goldwyer Formation|69312|4|Described|p1, p3, p7, p9, p13 fig 13-14|Middle Ordovician|Middle Ordovician|Canning Basin. Contains the best oil-prone source rocks in the basin. Up to 740m thick, but on average is generally around 400m thick. One of the three petroleum systems that forms the Larapintine Petroleum Supersystem. See also  p14 fig 15-16, p15, p17, p19, p23 fig 26-27, p24 fig 28, p25 fig 30, p26 fig 32-33, p27, p27 fig 34, p28 fig 36, p29, p30, p31. ||||Overlies the Willara Formation. Overlain by the Bongabinni Formation.|Interbedded calcareous shale, siltstone, argillaceous limestone and dolostone.|11-FEB-20
25928|Goldwyer Formation|69883|1|Redefined|p1-p7, p9-p10, p12-p14, p21-p22, p24|Llanvirn|Llanvirn|Canning Basin. The stratotype is the interval 848-1060m in Thangoo 1A (Elliot 1961; Burne et al, 1981). Two additional wells are nominated as reference sections (Solanum 1 283-563m and DD87SS7 1546-1780m). Deposited in an open marine shelf environment. Together with the Nita Formation forms a transgressive-regressive package. Intersected in at least 60 petroleum wells [see p3 for names] and a number of mineral drillholes. Assigned to supersequence A2. Contains potential petroleum source rocks which are considered to have excellent potential. This unit has an average thickness of 400m and the thickest section is 739m. Chronostratigraphy is based on conodonts ranging from Histiodella holodentata to the lower Pragmodus-Plectodina zones. Petrography, fossil assemblage, previous informal subdivisions and wireline logs discussed in detail. See also p27, p31, p33-p34, p36, p38, p43-p45, plate 1-4.||||Conformably overlies the Willara Formation and the Wilson Cliffs Sandstone. Conformably overlain by the Nita Formation.|Mudstones and carbonates which locally host biohermal carbonate build ups. This unit has in some areas undergone significant dolomitization. Includes 3 thin probable tuff beds.|27-FEB-20
25928|Goldwyer Formation|70061|6|Mentioned|Regional geology p8, p9|||Canning Basin. Oil-prone.||||||12-JUL-16
25928|Goldwyer Formation|70774|5|Briefly described|p4|Middle Ordovician|Middle Ordovician|Willara and Kidson Sub-basins, Canning Basin.||||Unconformably? Overlies the Wilson Cliffs Sandstone. Overlies the Willara Formation. Overlain by the Nita Formation.||
25928|Goldwyer Formation|71146|5|Briefly described|p6, p9, p12 fig 8, p26,  p43 fig 33, p43|Middle Ordovician|Middle Ordovician|Canning Basin. Deposited in shallow, warm water environments. Together with the Nita Formation hosts the giant Admiral Bay sulfide deposit.|466.9 +/- 0.1 Ma (IDTIMS)|||Overlies the Willara Formation. Overlain by the Nita Formation.|Carbonate, mudstone and volcanic rocks.|
25928|Goldwyer Formation|71171|5|Briefly described|p1-p2, p4, p20|||Amadeus Basin. Time equivalent to the Carranya Formation. Coeval with the Stairway Sandstone.||||||
25928|Goldwyer Formation|71592|5|Briefly described|Appendix A.|||Canning Basin.|512+/-4 Ma (MDA: U-Pb zircon SHRIMP)||||Fine-grained, quartz-rich sandstone with claystone intraclasts and various organic/phosphatic and calcareous fossil fragments, sparse tourmaline and zircon, and interstitial carbonate or clay.|
25928|Goldwyer Formation|71870|6|Mentioned|p1, p3, p5, p11-p12|Darriwilian|Darriwilian|Canning Basin. A petroleum source interval formed during the Larapintine petroleum supersystem.||||Overlies the Willara Formation. Overlain by the Nita Formation.||
25928|Goldwyer Formation|71894|5|Briefly described|p4, p6, p20, p31|Middle Ordovician|Middle Ordovician|Canning Basin.||||Overlies the Willara Formation. Overlain by the Nita Formation.|Carbonate and shale.|
25928|Goldwyer Formation|72497|5|Briefly described|p3 Fig.2.|Middle Ordovician|Middle Ordovician|Along with Nita Formation, Shown as occuring in parts of the Willara and Kidson Sub-basins, the Jurgurra and Barbwire Terraces and Broome Platform. Also shown as occuring in the Fitzroy Trough, Betty and Balgo Terraces and part of the Lennard Shelf and Margaret Terrace. Age given as Llanvirnian~= Darriwilian.||||Conformably overlies Wilsons Cliffs Sandstone and Willara Formation. Underlies Bongabinni Formation.||
25928|Goldwyer Formation|72499|5|Briefly described|p7 Fig.6.|Middle Ordovician|Middle Ordovician|Located in the Willara Sub-basin and the Broome Platform.||||Overlies Willara Formation and underlies Nita Formation. Shown as unconformably overlying Wilson Cliffs Sandstone.|Includes carbonate shales.|
25928|Goldwyer Formation|72500|5|Briefly described|p380-381, p389-394, p396, p399|Darriwilian|Darriwilian|Canning Basin.||||Overlies the Willara Formation. Overlain by the Nita Formation.||28-AUG-20
25928|Goldwyer Formation|72503|3|Fully described|p25-32, p37, p39-40, p50|early Darriwilian|middle Darriwilian|Canning Basin; widely distributed, only in subsurface. Four informal subdivisions; an upper shale (Goldwyer 4), a middle limestone (Goldwyer 3), and a lower shale (Goldwyer 1 and 2) (Haines, 2004). Lies at 1000-2500 m depth on the Broome Platform, and though to lie at >4000 m in the Fitzroy Trough. Confirmed maximum thickness: 736 m. Named after the Goldwyer No. 1 well. Type section is in the Thangoo No. 1A well, although the upper part of the unit is missing. As such, Haines (2004, p. 6, fig. 2) nominated two reference sections, the Solanum-1 well on the Barbwire Terrace, and mineral drillhole DD87SS7 in the Willara Sub-basin. Deposited in marine conditions ranging from intertidal to offshore; mainly in open and deeper water conditions. Carbonate lithologies are more abundant and locally dominant on platform and terrace areas. Lower and middle portion of the formation contains fossil biota recognized as the Histiodella serrata, Histiodella holodentata and Eoplacognathus pseudoplanus biozones [see article for details]. Age is based on this assemblage. The presence of several biogeographically distinctive conodont species indicates a connection with the Sino-Korean Craton. [Article discusses 25 conodonts from two drill core sections on the Broome Platform].||||Conformably underlain by Willara Formation. Conformably[?] overlain by Nita Formation. Equivalent[?] to Carranya Formation.|Consists predominantly of mudstone and carbonate with minor sandstone. Significant dolomitization has occurred in parts. Middle portion includes thin, intercalated shallow marine bioclastic to oolitic carbonate rocks and transgressive shales.|
25928|Goldwyer Formation|72504|6|Mentioned|Figure 3|||Canning Basin, Broome Platform. Intersected in Pictor 1 and Canopus 1 drillholes, and probably Looma 1, Robert 1, Fruitcake 1, Missing 1.||||||18-MAR-20
25928|Goldwyer Formation|73117|5|Briefly described|p3, p30, p32, p141-142|Middle Ordovician|Middle Ordovician|Canning Basin. Hydrocarbon source interval.||||Underlain by Willara Formation. Unconformably underlain[?] by Wilson Cliffs Sandstone. Overlain by Nita Formation and Cobb Formation.|Dominantly carbonate-shale, marl.|
25928|Goldwyer Formation|73344|5|Briefly described|p4, p6, p8, p40, p42, Pl.1-4|Darriwilian|Darriwilian|Canning Basin, subsurface. Part of supersequence A2. Records a major transgressive event. Biostratigraphy suggests the unit may be unconformably underlain by Wilson Cliffs Sandstone in some wells. Includes the H. holodenata biozone.||||Underlain by Willara Formation. Unconformably underlain by Wilson Cliffs Sandstone. Overlain by Nita Formation. Equivalent to Carranya Formation.||
25928|Goldwyer Formation|73345|6|Mentioned|p227|Middle Ordovician|Middle Ordovician|Canning Basin, widespread. Potentially correlative to Barnicarndy Formation.||||||
25928|Goldwyer Formation|73346|6|Mentioned|p3, p25-27, App.1 p34|Darriwilian|Darriwilian|Canning Basin. Deposited in shallow marine environments. May be age equivalent to Cobb Formation. Notably sand-free across most of its range.|||||Mostly sand-free but contains fine-grained calcareous sandstone in some places.|
26587|Gombugurra Rhyolite|30388|4|Described|Table 1|||Middle Proterozoic age. Table 1 on P9-10||||||
26587|Gombugurra Rhyolite|30390|4|Described|p68|||See also P69-72||||||
26587|Gombugurra Rhyolite|30944|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
26587|Gombugurra Rhyolite|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
26587|Gombugurra Rhyolite|36551|6|Mentioned|Table 31|||||||||
26587|Gombugurra Rhyolite|36886|4|Described|p198|||||||||
26587|Gombugurra Rhyolite|50607|5|Briefly described|p3.2|||Geological Province: Musgrave Block. Of the Cassidy Group.||||||
26587|Gombugurra Rhyolite|67375|5|Briefly described|p38 Table 1, p49. |Mesoproterozoic|Mesoproterozoic|||Unit in Cassidy Group.||Overlies Wururu Rhyolite. Is overlain by Gurgadi Basalt.|Dark-grey, feldspar-phyric rhyolite with very fine-grained groundmass; massive, flow-banded or spherulitic|
26587|Gombugurra Rhyolite|67553|5|Briefly described|p40,51|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Talbot Sub-basin, Bentley Sub-basin. Only present in the area of the WARBURTON RANGE 1:100 000 map sheet, and thins to the east. ||Unit of Cassidy Group.||Overlain by Gurgadi Basalt. Underlain by Wururu Rhyolite.||
26587|Gombugurra Rhyolite|68995|5|Briefly described|p7 Fig.3, p9 Tb. 1, p18, p22|Stenian|Stenian|Estimated 110m thick. Western Talbot Sub-basin. Metamorphism discussed.||Cassidy Group||Overlies the Wururu Rhyolite. Overlain by the Gurgadi Basalt.|Rhyolitic lava flows or rheomorphic ignimbrites.|
26587|Gombugurra Rhyolite|69091|6|Mentioned|p71 Fig.4.14|||Talbot Sub-basin||Cassidy Group||||
26587|Gombugurra Rhyolite|69153|6|Mentioned|GEOCHRON/174691.1.pdf and 174690.1.pdf|||||Cassidy Group||||
26587|Gombugurra Rhyolite|69729|6|Mentioned|p82|||Bedrock of Talbot Sub-basin.||Cassidy Group.||||
26587|Gombugurra Rhyolite|70095|5|Briefly described|p16-17|||Geological province: Musgrave Province. Talbot Sub-basin, Of Bentley Basin. Thickness of rhyolitic package: 0.11km, over 30km in strike length and interpreted minimum volume of 99km3.||Unit of Cassidy Group.||Overlain by Gurgadi Basalt. Underlain by Wururu Rhyolite.||
26587|Gombugurra Rhyolite|70134|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Cassidy Group.||Overlies Wururu Rhyolite. Is overlain by Thomas Rhyolite.|Microcrystalline, feldspar-porphyritic, flow-banded rhyolite containing up to 7% euhedral feldspar, phenocrysts up to 3mm in size, locally spherulitic (section only).|
26587|Gombugurra Rhyolite|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Cassidy Group.||Overlies Wururu Rhyolite. Is overlain by Gurgdi [mis-spelling of Gurgadi] Basalt.|Microcrystalline, feldspar-porphyritic, flow-banded rhyolite containing up to 7% euhedral feldspar phenocrysts up to 3mm in size; locally spherulitic.|12-NOV-15
26587|Gombugurra Rhyolite|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic||1047 Ma - 1077 Ma (Inferred)|Cassidy Group|||Microcrystalline, feldspar-porphyritic, flow banded rhyolite containing up to 7% euhedral feldspar phenocrysts up to 3 mm in size; locally spherulitic|
26587|Gombugurra Rhyolite|70793|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv.|1077-1047 Ma (inferred)|Unit of Cassidy Group.|||Microcrystalline, feldspar-porphyritic, flow-banded rhyolite containing up to 7% euhedral feldspar phenocrysts up to 3 mm in size; locally spherulitic|
26587|Gombugurra Rhyolite|71211|6|Mentioned|p216|||||Cassidy Group||||
26587|Gombugurra Rhyolite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv.|1077-1047 Ma (inferred)|Unit of Cassidy Group.|||Microcrystalline, feldspar-porphyritic, flow-banded rhyolite containing up to 7% euhedral feldspar phenocrysts up to 3 mm in size; locally spherulitic|
26587|Gombugurra Rhyolite|72443|6|Mentioned|p738-739|||Talbot Sub-basin.||Cassidy Group||||
36003|Gooche Gneiss|50292|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: c. 1770Ma.  Geological Province: Gascoyne Complex.||||||07-NOV-08
36003|Gooche Gneiss|61262|2|Defined|p458 App., See also p445, p447 Fig. 4.|Paleoproterozoic|Paleoproterozoic|Series of small inliers faulted against Pooranoo Metamorphics, and inclusions in Durlacher Supersuite granites. Biotite granodiorite and monzogranite, and pegmatite-banded augen gneiss. Age: 1776+-8Ma (age of igneous crystallisation of precursor granite).||||||07-NOV-08
36003|Gooche Gneiss|63470|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Moorarie Supersuite. Age: c.1830-1780Ma.  Geological Province: Gascoyne Complex. Strongly foliated porphyritic granodiorite and monzogranite, and augen gneiss.||||||07-NOV-08
36003|Gooche Gneiss|63866|5|Briefly described|p160|||Forms basement to the Mangaroon Zone. SHRIMP age is interpreted as the age of igneous crystallisation and was derived from Nelson (2002).|1776 +/- 8 Ma (SHRIMP U-Pb zircon)|Moorarie Supersuite|||Foilated, porphyritic biotite granodiorite or monzogranite to pegmatite-banded augen gneiss.|
36003|Gooche Gneiss|63869|4|Described|p5, p12-13, p21, p22-23, p25-26, Plate 1|Paleoproterozoic|Paleoproterozoic|Forms basement to the Mangaroon Zone of the Gascoyne Complex. [Said to be] Defined on EDMUND sheet (Martin et al., 2002) where it forms several rafts in the Pimbyana Granite [showing the area of outcrop of a unit on a map is not sufficient to define it]. Outcrops as small inliers in Pooranoo Metamorphics; contacts are tectonic. Several plutons dated; this one is igneous crystallisation age of a precursor granite.|1776 +/- 8 Ma SHRIMP U/Pb (GSWA, 2005).|Unit in Moorarie Supersuite.|||Foliated, porphyritic biotite granodiorite or monzogranite, to a pegmatite-banded augen gneiss.|06-MAR-18
36003|Gooche Gneiss|64580|4|Described|map legend||Paleoproterozoic|Of Moorarie Supersuite. Strongly foliated, porphyritic granodiorite and monzogranite, and augen gneiss.||||||15-DEC-08
36003|Gooche Gneiss|64725|6|Mentioned|p58 Fig.2.|||Capricorn Orogen.|1800-1750 Ma.|||||
36003|Gooche Gneiss|65830|6|Mentioned|p31, p33, Plate 2|Statherian|Statherian|A deformed part of Moorarie Supersuite. Small inliers tectonically interleaved with Pooranoo Metamorphics.|1776 +/- 8 Ma (GSWA, 2006).|||||
36003|Gooche Gneiss|66299|4|Described|p144, p172, p236.|Paleoproterozoic|Paleoproterozoic|Mangaroon Zone, Gascoyne Province. Forms several elongate rafts in the Pimbyana Granite and a series of small inliers in the Pooranoo Metamorphics. Typically weathered, but commonly well exposed as whalebacks and pavements.|1776 +/- 8 Ma.|Unit in Moorarie Supersuite.||Intruded by dykes and veins of Yangibana Granite. In faulted contact with gneiss of Pooranoo Metamorphics.|Foliated, porphyritic biotite metagranodiorite and metamonzogranite; pegmatite-banded augen gneiss; K-feldspar phenocrysts are round and up to 3 cm in diameter.|
36003|Gooche Gneiss|66950|6|Mentioned|p11|Orosirian|Orosirian|||Of the Moorarie Supersuite.||||
36003|Gooche Gneiss|69028|5|Briefly described|Map Legend|Statherian|Orosirian|Gascoyne Province.||Of the Moorarie Supersuite.|||Strongly foliated, porphyritic metagranodiorite and metamonzogranite, and augen gneiss.|07-MAY-14
36003|Gooche Gneiss|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Age derived from augen gneiss sample and corresponds to crystallisation of granite protolith (169058.1.pdf)|1776 Ma +/- 8 Ma (SHRIMP) |Moorarie Supersuite|||Strongly foliated, porphyritic metagranodiorite and metamonzogranite, and augen gneiss|
36003|Gooche Gneiss|69185|4|Described|500k_geologyp08_lut.csv||Paleoproterozoic|Geological Province: Pilbara Craton.||Unit of Moorarie Supersuite.|||Strongly foliated, porphyritic granodiorite and monzogranite, and augen gneiss|
36003|Gooche Gneiss|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 169058.1.pdf|1776 Ma||||Strongly foliated, porphyritic metagranodiorite and metamonzogranite, and augen gneiss.Porphyritic granite.|
36003|Gooche Gneiss|70814|6|Mentioned|p66|||||||||
36003|Gooche Gneiss|71869|5|Briefly described|p7, app p13|||Capricorn Orogen.|1776 +/- 8 Ma (Igneous crystalisation age)|Moorarie Supersuite|||Augen orthogneiss.|17-AUG-22
67862|Goodia Monzogranite|60076|5|Briefly described|p45 App. 1|||[Agmgi]   Equigranular, fine- to medium-grained biotite monzogranite to granodiorite.||||||
67862|Goodia Monzogranite|65258|5|Briefly described|Map Legend|Archaean|Archaean|Equigranular, fine- to medium-grained biotite monzogranite to granodiorite with strongly foliated margins.||||||16-JUN-09
67862|Goodia Monzogranite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Fine- to medium-grained, equigranular biotite monzogranite to granodiorite; strongly foliated margins.||||||07-FEB-11
67862|Goodia Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Fine- to medium-grained, equigranular biotite monzogranite to granodiorite; strongly foliated margins.|06-AUG-15
67862|Goodia Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Fine- to medium-grained, equigranular biotite monzogranite to granodiorite; strongly foliated margins.|
67862|Goodia Monzogranite|70802|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton.|||||Fine- to medium-grained, equigranular biotite monzogranite to granodiorite; strongly foliated margins|
67862|Goodia Monzogranite|71270|4|Described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton.|||||Fine- to medium-grained, equigranular biotite monzogranite to granodiorite; strongly foliated margins|
79009|Goonetarra Granodiorite|70226|5|Briefly described|Map legend.|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Carton.|c. 2749 Ma (Fletcher and McNaughton, 2002).|Rothsay Suite.|||Equigranular monzogranite to syenogranite, undeformed; foliated biotite (or K-feldspar megacrystic biotite) metamonzogranite, commonly strongly foliated; layered (biotite) tonalite gneiss, crosscut or intruded.|16-DEC-15
79009|Goonetarra Granodiorite|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton. Six facies are mapped separately.|c.2749 Ma.|Rothsay Suite.|||Monzogranite and metamonzogranite: K-feldspar-porphyritic to megacrystic; equigranular and undeformed or foliated. Layered biotite tonalite gneiss. Foliated biotite metamonzogranite.|
79009|Goonetarra Granodiorite|70796|5|Briefly described|100k_geologyl_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 155822.1.pdf, Badja100_2240_stratig.pdf, Yalgoo100_2241_stratig.pdf. Numerous additional lithologies are discussed.|2749 +/ 4 Ma (Isotopic)|Rothsay Suite|||Foliated biotite metamonzogranite, with local Kfeldspar phenocrysts; Kfeldspar megacrystic biotite metamonzogranite, biotite tonalite gneiss, layered tonalite gneiss, equigranular mozngranite to syenogranite.|
79009|Goonetarra Granodiorite|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). Sample GSWA 155822 (monzogranite gneiss, this study) yielded a weighted mean 207Pb/206Pb date of 2749+\-4 Ma, interpreted to be magmatic age of the monzogranite protolith. Sample GSWA 155582 (metamonzogranite, this study) yielded a weighted mean 207Pb/206Pb date of 2752+\-13 Ma, interpreted to be magmatic age of the metamonzogranite. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeol_lut.csv.|2752-2749 Ma (inferred)|Unit of Rothsay Suite.|||Equigranular monzogranite to syenogranite; common magmatic foliation, rafts of migmatitic tonalite; k-feldspar-porphyritic to megacrystic monzogranite; magmatic foliation; foliated to megacrystic biotite metamonzogranite, layered tonalite gneiss.|
79009|Goonetarra Granodiorite|73023|5|Briefly described|p2-3|Neoarchaean|Neoarchaean|Surrounding the core, this unit constitutes the bulk of the Yalgoo Dome in the western Murchison Domain, Youanmi Terrane, Yilgarn Craton.|2760-2740 Ma.|||Surrounds Kynea Tonalite. Is intruded by Bald Rock Supersuite.||
79009|Goonetarra Granodiorite|73410|5|Briefly described|p2, 4-5|||The most voluminous granite in the Yalgoo dome, Youanmi Terrane.|2752 +/- 13 Ma (Lu et al. 2013).|Rothsay Suite.||||
34910|Gooragoora Formation|22905|4|Described|p52 Fig. 2, p53|Mesoproterozoic|Mesoproterozoic|Of Edmund Group. Supersedes Gooragoora Sandstone Member.  Max thickness: 150 m. Conformably overlain by Blue Billy Formation. Conformably overlies Irregully Formation.||||||25-JAN-06
34910|Gooragoora Formation|24115|4|Described|p4 Fig.2|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group. Maximum Thickness: 150m. Overlies the Irregully Formation. Overlain by the Blue Billy Formation. Geological Province: Edmund Basin.||||||
34910|Gooragoora Formation|24183|2|Defined|p10|Calymmian|Statherian|Formerly known as the Gooragoora Sandstone Member (Daniels 1970). Max. Thickness: 250m. Overlain by the Blue Billy Formation. Overlies the Irregully Formation. Age: 1620-1462 Ma.||||||21-MAR-11
34910|Gooragoora Formation|24544|4|Described|p44 Fig.32|Mesoproterozoic|Mesoproterozoic|Superseded Gooragoora Sandstone. Of Edmund Group. Overlies Irregully Formation. Overlain by Blue Billy Formation.||||||
34910|Gooragoora Formation|50225|4|Described|p387 Fig. 2, p393|||Of Edmund Gp. Supersedes Goorgoora Sandstone of former Edmund Subgroup. Predominantly sandstone + siltstone locally interbedded with sifnificant amounts of carbonate. Conformably overlies Irregully Fm. Max. thick: 150m.||||||07-FEB-11
34910|Gooragoora Formation|50292|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Geological Province: Edmund Basin.  Of the Edmund Group (Bangemall Supergroup). Overlies: Irregully Formation.  Underlies: Blue Billy Formation.||||||07-NOV-08
34910|Gooragoora Formation|50312|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Edmund Group. Overlies Irregully Formation. Geological Province: Edmund Basin. Fine- to course-grained sandstone, and siltstone; minor conglomerate, dolostone, and dolomitic siltstone.||||||31-MAY-04
34910|Gooragoora Formation|50313|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup).  Geological Province: Edmund Basin.  Underlies: Blue Billy Formation.  Overlies: Irregully Formation.||||||07-NOV-08
34910|Gooragoora Formation|50380|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin.||||||07-NOV-08
34910|Gooragoora Formation|63866|5|Briefly described|p162|||||Edmund Group||||
34910|Gooragoora Formation|63869|4|Described|p28-31, p59, Plate 1|Calymmian|Statherian|Originally defined as a Member of Irregully Formation by Daniels (1970) and Muhling and Brakel (1985); raised to Formation status by Martin and Thorne (2002). 150-250 m thick. Hosts stratabound base metal mineralisation.|c.1620-1465 Ma.|Unit in Edmund Group.||Overlies Irregully Formation, possibly unconformably. Is overlain by Blue Billy Formation and disconformably by Kiangi Creek Formation.|Medium- to thick-bedded, fine to very coarse grained sandstone; lesser conglomerate and planar-laminated siltstone; local dolostone.|
34910|Gooragoora Formation|64287|5|Briefly described|p34 Fig. 2|||Sandstone, siltstone unit on EDMUND sheet.||||||07-FEB-11
34910|Gooragoora Formation|64580|4|Described|map legend||Mesoproterozoic|Of Edmund Group. Siltstone and mudstone; sandstone, and dolostone; locally sulfidic.||||||
34910|Gooragoora Formation|64728|5|Briefly described|p95 Fig.2, p96, pp99-100. |Mesoproterozoic|Mesoproterozoic|Deltaic to deep marine siliciclastic and carbonate facies. Unimodal southwards-directed paleocurrents.|Maximum depositional age around 1733 +/- 12 Ma.|Unit in Edmund Group.||Overlies Irregully Formation. Is overlain by Blue Billy Formation.|Thick-bedded, medium-grained quartz sandstone.|
34910|Gooragoora Formation|65830|4|Described|p4, p5, p9; Plates 1,2|Calymmian|Statherian|Interpreted to have been deposited by the progradation of coarse-grained deltaic sediments during a period of high or rising sea level.||Of the Edmund Group||Disconformably overlies Irregully Formation. Overlain by the Blue Billy Formation. Disconformably overlain by the Kiangi Creek Formation.|Consists mainly of medium- to thick-bedded, trough cross-stratified, very coarse to fine-grained sandstone with lesser amounts of conglomerate, planar-laminated siltstone, and dolostone.|
34910|Gooragoora Formation|66241|6|Mentioned|pp1-4. |||||Unit in Edmund Group.||Overlies Irregully Formation. Is overlain by Blue Billy Formation.||
34910|Gooragoora Formation|69003|5|Briefly described|p34|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||Edmund Group.||Overlies Irregully Formation. Is overlain by Blue Billy Formation.||
34910|Gooragoora Formation|69024|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin. Includes an unnamed subunit of medium- to thick-bedded sandstone and siltstone, mapped separately.||Of the Edmund Group.||Conformably overlies Irregully Formation. Overlain conformably by Blue Billy Formation.|Fine- to coarse-grained sandstone, and siltstone; minor conglomerate, dolostone, and dolomitic siltstone; medium- to thick-bedded sandstone and siltstone.|05-MAY-14
34910|Gooragoora Formation|69027|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Of the Edmund Group.||Underlain by the Irregully Formation. Overlain by the Blue Billy Formation.|Fine- to coarse-grained sandstone and siltstone; minor conglomerate, dolostone, and dolomitic siltstone.|05-MAY-14
34910|Gooragoora Formation|69028|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin. Mapped with Blue Billy and Cheyne Springs Formations as one unit.||Of the Edmund Group.|||Siltstone and mudstone, sandstone and dolostone; locally sulphidic.|06-MAY-14
34910|Gooragoora Formation|69166|4|Described|geologyp_lut.csv|Mesoproterozoic|Paleoproterozoic|Age derived from quartz sandstone sample (148970.1.pdf)|1749 Ma +/- 9 Ma(SHRIMP)|Edmund Group||Conformably overlies Irregully Formation, Conformably overlain by Blue Billy Formation|Fine- to coarse-grained sandstone and siltstone; minor conglomerate, dolostone, and dolomitic siltstone|
34910|Gooragoora Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|||Part of Edmund Group, Depositiional package 2.||Unit of Edmund Group.||||
34910|Gooragoora Formation|69596|6|Mentioned|p12 Fig.7|||Edmund Basin.||Edmund Group.||||
34910|Gooragoora Formation|70019|5|Briefly described|p93-94|Mesoproterozoic|Mesoproterozoic|Geological province: Gascoyne Province, Capricorn Orogen.||Unit of Edmund Group.||Overlain by Blue Billy Formation. Underlain by Irregully Formation.||
34910|Gooragoora Formation|70127|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Edmund Group.|||Fine- to very coarse-grained sandstone and siltstone; minor conglomerate, dolostone and dolomitic siltstone.|
34910|Gooragoora Formation|70138|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin.||Edmund Group.||Overlies Irregully Formation. Is overlain by Kiangi Creek Formation and is intruded by Narimbunna Dolerite.|Fine- to very coarse-grained sandstone and siltstone; minor conglomerate, dolostone and dolomitic siltstone.|
34910|Gooragoora Formation|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 148970.1.pdf West Australian Craton, Edmund Basin|1679-1465 Ma|Edmund Group||Conformably overlies Irregully Formation, conformably overlain by Blue Billy Formation|Fine to very coarse grained and medium to thick bedded quartz sandstone and siltstone; minor conglomerate, dolostone and dolomitic siltstone.|
34910|Gooragoora Formation|70814|4|Described|p3, p5, p8-p10, p12|Statherian|Statherian|Edmund Basin. Together with the Blue Billy and Cheyne Springs Formations forms Depositional Package 2 of the Edmund Group. Together with the Irregully Formation hosts the Abra polymetallic deposit. Generally up to 250m thick. Interpreted to have been deposited in a deltaic to shallow-marine shelf environment. Age is derived from the maximum age of the underlying Mount Augustus Sandstone and extensive hydrothermal alteration and mineralization of this unit at the Abra polymetallic deposit. See also p20, p22, p24, p27, p31, p41-p42, p47, p55.|1679-1610 Ma|Edmund Group||Conformably overlies the Irregully Formation. Conformably overlain by the Blue Billy Formation.|Fine-grained to very coarse-grained quartz sandstone, feldspathic sandstone and siltstone together with minor conglomerate and dolomite.|
34910|Gooragoora Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone, conglomerate, crystalline dolostone/dolomite|
34910|Gooragoora Formation|72705|5|Briefly described|p3-4|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||Edmund Group.||Conformably overlies Irregully Formation. Is overlain by Blue Billy Formation.|Siltstone grading upwards to sandstone; deltaic (shallow marine) environment.|
34910|Gooragoora Formation|73102|6|Mentioned|p21|||Intruded by a quartz dolerite dyke dated by U-Pb SHRIMP at 1081+/- 27 Ma (crystallisation age).||Edmund Group, lower.||Intruded by Kulkatharra Dolerite.|Includes sandstone and siltstone.|
23629|Goose Hole Group|14019|4|Described|p21|Middle Cambrian|Middle Cambrian|Contains all the Middle and Late Cambrian sedimentary rocks of the Ord Basin.  Subdivided into the Negri (below) and Elder (above) Subgroups.  Limestone, sandstone.  Max. thickness: 700m.  Geological Province: Ord Basin.  See also p3 Fig. 2.||||||
23629|Goose Hole Group|22547|3|Fully described|p30||Early Cambrian|Geological province: Ord Basin. Age: 525 Ma.||||||14-NOV-06
23629|Goose Hole Group|22814|5|Briefly described|fig2|Middle Cambrian|Middle Cambrian|||||||
23629|Goose Hole Group|23621|5|Briefly described|p36|Late Cambrian|Middle Cambrian|See also page 9 Table 1. Geological Province: Ord Basin.||||||
23629|Goose Hole Group|23622|5|Briefly described|Map Legend|Cambrian|Cambrian|Of Goose Hole Group. Geological Province: Ord Basin.||||||
23629|Goose Hole Group|24503|5|Briefly described|Map legend|Ordovician|Middle Cambrian|Sandstone, limestone, stromatolitic limestone, siltstone and mudstone.  Geological Province: Ord Basin.||||||01-FEB-16
23629|Goose Hole Group|40993|6|Mentioned|Fig.1|||||||||
23629|Goose Hole Group|41598|5|Briefly described|p412|||||||||
23629|Goose Hole Group|41840|3|Fully described|p40|||||||||
23629|Goose Hole Group|41864|4|Described|p15|||||||||
23629|Goose Hole Group|41865|6|Mentioned|Map legend|Late Cambrian|Middle Cambrian|||||||
23629|Goose Hole Group|41866|6|Mentioned|Map legend|Late Cambrian||||||||
23629|Goose Hole Group|43299|5|Briefly described|Map Legend||Cambrian|||||||
23629|Goose Hole Group|43853|5|Briefly described|Map Legend||Ordian|||||||
23629|Goose Hole Group|43855|5|Briefly described|Map Legend||Middle Cambrian|||||||
23629|Goose Hole Group|44230|5|Briefly described|Map Legend||Middle Cambrian|||||||
23629|Goose Hole Group|44868|5|Briefly described|Map Legend|Boomerangian|Ordian|||||||
23629|Goose Hole Group|60419|5|Briefly described|p1|Late Cambrian|Middle Cambrian|Max. thickness: 700 m. Conformably overlies Antrim Plateau Volcanics. Geological Province: Ord Basin.||||||
23629|Goose Hole Group|60519|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Includes: Negri Subgroup, Elder Subgroup. Geological Province: Ord Basin.||||||03-NOV-04
23629|Goose Hole Group|60589|5|Briefly described|Map legend|Late Cambrian|Middle Cambrian|Limestone, sandstone.  Unconformably overlies the Antrim Plateau Volcanics.  Geological Province: Ord Basin.||||||
23629|Goose Hole Group|64443|6|Mentioned|p40|||Of Ord Basin. Correlative of Barkly Group, Georgina Basin.||||||
23629|Goose Hole Group|64580|4|Described|map legend|Furongian|Middle Cambrian|Undivided; sandstone, siltstone, minor limestone (in part stromatolitic) and mudstone; includes HEADLEYS and LINNEKAR LIMESTONES, NELSON SHALE, PANTON FORMATION, and EAGLE HAWK and OVERLAND SANDSTONES.||||||09-DEC-08
23629|Goose Hole Group|67151|5|Briefly described|Map legend.|Cambrian|Cambrian|Ord Basin.|||Includes Headleys Limestone.|||
23629|Goose Hole Group|67860|4|Described|p416 Fig.4-84, p417, p419 Tb. 4-18|Cambrian|Cambrian|See also p421 fig 4-86. 180-700m thick shallow marine to fluvial sediments. Appears also as Goosehole Group.|||Includes Negri and Elder Subgroups.|Conformably overlies Antrim Plateau Volcanics.|Siltstone and sandstone; minor limestone.|
23629|Goose Hole Group|69099|4|Described|GEOL_LUT_CSV files + geochron files|Furongian|Stage 5|Ord Basin? Also says grouped as Cambrian-Ordovician sedimentary rocks, Southern Bonaparte Basin.|||Includes Elder Subgroup, Negri Subgroup.||Sandstone, siltstone, minor limestone (in part stromatolitic) and mudstone.|31-JUL-15
23629|Goose Hole Group|69165|5|Briefly described|100k_interpgeop_lut.csv|Furongian|Cambrian|See also 500k_geologyp08_lut.csv.|||Includes Elder Subgroup, Negri Subgroup||Undivided; sandstone, siltstone, minor limestone (in parts stromatolitic) and mudstone.|
23629|Goose Hole Group|69443|6|Mentioned|p28:21|||Ord Basin.||||Correlated with Barkly Group.||12-JUL-16
23629|Goose Hole Group|69448|5|Briefly described|p33:1-8|Late Cambrian|Middle Cambrian|Traves (1955); Mory and Beere (1985, 1988). Contains the entire Ord Basin succession in NT. Total thickness c.700m. Displaced by  the NW-trending Negri Fault.|||Negri, Elder Subgroups.|Is overlain unconformably by Mahony Group.||12-JUL-16
23629|Goose Hole Group|69634|4|Described|GEOL_LUT_CSV files|Furongian|Stage 5|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|509-485.4 Ma (Inferred)||Includes Elder Subgroup, Negri Subgroup.||Sandstone, siltstone, minor limestone (in part stromatolitic) and mudstone|
23629|Goose Hole Group|69673|6|Mentioned|p192|||700m thick.|||Includes Negri Subgroup, Elder Subgroup|||
23629|Goose Hole Group|70154|5|Briefly described|100k_interpgeop_lut.csv|Ordovician|Cambrian|See also 500k_interpgeop_lut.csv.|485-509 Ma||Includes Elder Subgroup, Negri Subgroup||Sandstone, siltstone, minor limestone and mudstone.|
23629|Goose Hole Group|70655|5|Briefly described|Map Legend|Cambrian|Cambrian|Ord Basin.|||Includes Headleys Limestone.|||
23629|Goose Hole Group|70826|6|Mentioned|p7 tbl 3|Cambrian|Cambrian|Ord Basin.||||||
23629|Goose Hole Group|70851|6|Mentioned|p17-p18|||||||||
23629|Goose Hole Group|71146|5|Briefly described|p6|Cambrian|Cambrian|Ord Basin.|||Includes the Negri and Elder Subgroups.|||
23629|Goose Hole Group|71267|4|Described|GEOL_LUT_CSV files|Furongian|Stage 5|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny (450-295 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|508-485.4 Ma (inferred)||Includes Elder Subgroup, Negri Subgroup.||Sandstone, siltstone, minor limestone (in part stromatolitic) and mudstone|
23629|Goose Hole Group|71800|4|Described|p25-p26|Late Cambrian|Middle Cambrian|Ord Basin. Approximately 700m thick in the Hardman syncline.|||Includes the Negri Subgroup and the Elder Subgroup.|Conformably overlies the Antrim Plateau Volcanics.||
23629|Goose Hole Group|72034|5|Briefly described|500k_interpgeop16_lut|Furongian|Stage 5|Ord Basin.|||||Sandstone, siltstone, minor limestone (in part stromatolitic) and mudstone.|
23629|Goose Hole Group|73255|6|Mentioned|p533 Fig.1, p534 Fig.2|Cambrian|Cambrian|Contains Redlichia forresti, Gudugawan hardmanae and Xystridura negrina trilobite fossils.|||Headleys Limestone, Nelson Shale, Linnekar Limestone, Panton Formation, Eagle Hawk Sandstone, Overland Sandstone.|Overlies the Antrim Plateau Basalt, disconformably underlies the Mahony Group.|Includes carbonate rocks.|
23630|Gooseneck Member|13194|4|Described|p390 Tb. 4-16|||Type Section: Elf Aquitaine drill hole WBS 5048 15o27'S 128o59'E (77-199m). 0-100m thick open marine shelf deposits.  Correlated to top 216m of type section of Burt Range Formation.||Burt Range Formation, at Sorby Hills||Overlies Knox Siltstone Member with local disconformably. Overlies Cockatoo Group (disconformably).|Limestone, sandy dolomite and silty sandstone, basal peloidal dolomite breccia.|
23630|Gooseneck Member|40792|2|Defined|p177|early Tournaisian|early Tournaisian|||||||
23630|Gooseneck Member|41864|5|Briefly described|p103|||||||||
23630|Gooseneck Member|42175|5|Briefly described|p197|||||||||
23630|Gooseneck Member|45169|6|Mentioned|Fig.4|||||||||
23630|Gooseneck Member|64694|6|Mentioned|p235, p238, p252-253, p254 Fig.12|Tournaisian|Tournaisian|||Unit in Burt Range Formation.||||
79199|Gora Hill Suite|70182|4|Described|p9, p33-34, p38-41, p43-47|Mesoproterozoic|Mesoproterozoic|New name, after Gora Hill. Refers to Recherche Supersuite granites grouped by silica content into granodiorites (SiO2 < 64 wt%), monzogranites (SiO2 64-70.5 wt%) and syenogranites (SiO2 > 70.5 wt%). East Albany-Fraser Orogen. Geochemistry detailed; magmatic evolution discussed.|c.1330 Ma to 1283 Ma.|Recherche Supersuite.|||Syenogranite, monzogranite, granodiorite.|13-APR-18
79199|Gora Hill Suite|70735|6|Mentioned|p29, 37, 42|||Albany-Fraser Orogen. Derived through melting of Fraser gabbro-like mafic rocks and mixing with silicic crust.|||||Typically metaluminous granites, granodiorites.|
79199|Gora Hill Suite|70802|4|Described|250k_pre_mesozoic_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen. Events: Albany-Fraser Orogeny Stage I (1330-1260 Ma);  Albany-Fraser Orogeny (1330-1140 Ma); Albany-Fraser Orogeny Stage II (1225-1140 Ma). Magmatism coinciding with Stage I Albany-Fraser Orogeny (Spaggiari et al., 2014). Typically foliated or gneissic, and metamorphosed to amphibolite or granulite facies during either Stage I or II (or both) Albany-Fraser Orogeny (Spaggiari et al., 2014). Sample GSWA 194836 (metamonzogranite) yielded weighted mean 207Pb*/206Pb* ages of 1323+\-5 Ma and 1187+\-8 Ma, interpreted as magmatic crystallisation age of the monzogranite, and high-grade metamorphism respectively.|1330-1283 Ma (inferred)|Unit of Recherche Supersuite.|||Granodiorite, monzogranite and syenogranite gneiss|
79199|Gora Hill Suite|70813|5|Briefly described|p6, p19-p21, p24-p26|||Fraser zone. Intrudes the eastern Nornalup Zone.|c. 1330 Ma|Recherche Supersuite|||Metaluminous granites and granodiorites.|
79199|Gora Hill Suite|72059|5|Briefly described|p67|Ectasian|Ectasian|Geological province: Fraser Zone, Albany-Fraser Orogen.||Unit of Recherche Supersuite.||||
79199|Gora Hill Suite|72710|5|Briefly described|p8-9.|Ectasian|Ectasian|One of two geochemically distinct suites that form the Recherche Supersuite. Said to be formed from  a mixture of Archean and Paleoproterozoic crust.|1330 Ma to 1276 Ma.|Recherche Supersuite|||Includes granitic rocks.|
31791|Gordons Gorge Granite|22547|4|Described|p12||Orosirian|Of the Paperbark supersuite.||||||14-NOV-06
31791|Gordons Gorge Granite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.||||||07-NOV-08
31791|Gordons Gorge Granite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1850Ma. Geological province: Kimberley Province (East).||||||07-FEB-11
31791|Gordons Gorge Granite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
31791|Gordons Gorge Granite|43853|5|Briefly described|Map Legend||Proterozoic|||||||
31791|Gordons Gorge Granite|44230|5|Briefly described|Map Legend||Proterozoic|||||||
31791|Gordons Gorge Granite|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite.||||||07-NOV-08
31791|Gordons Gorge Granite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Paperbark Supersuite|||Coarse-grained, biotite(-hornblende) monzogranite and syenogranite with rapakivi texture.|31-JUL-15
31791|Gordons Gorge Granite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Paperbark Supersuite|||Coarse grained, biotite-hornblende monzogranite and syenogranite with rapakivi texture.|
31791|Gordons Gorge Granite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone.|1864-1852 Ma (Inferred)|Unit of Paperbark Supersuite.|||Coarse-grained, biotite(-hornblende) monzogranite and syenogranite with rapakivi texture|
31791|Gordons Gorge Granite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1852-1862 Ma|Paperbark Supersuite|||Coarse grained biotite-hornblende monzogranite and syenogranite with rapakivi texture.|
31791|Gordons Gorge Granite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1864-1852 Ma (inferred)|Unit of Paperbark Supersuite.|||Coarse-grained, biotite(-hornblende) monzogranite and syenogranite with rapakivi texture|
31791|Gordons Gorge Granite|72437|5|Briefly described|p88-89|||Lamboo Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Porphyritic biotite monzogranite.|
27160|Gorge Creek Group|22441|6|Mentioned|p14|||Pilbara Craton. Overlies Kangaroo Caves Formation||||||
27160|Gorge Creek Group|22449|6|Mentioned|Fig27 P26||Archean|Age of unit is <3240 Ma||||||07-NOV-08
27160|Gorge Creek Group|22473|6|Mentioned|p 4|||Pilbara Craton||||||
27160|Gorge Creek Group|22615|5|Briefly described|p 5|||||||||
27160|Gorge Creek Group|22642|6|Mentioned|485|||Geol province Pilbara Craton. Alias Sloansville Sub Group. Underlying unit Warrawoona Group||||||
27160|Gorge Creek Group|22715|5|Briefly described|table7,fig7,p216|Archean|Archean|Age: 3270-3200Ma||||||07-NOV-08
27160|Gorge Creek Group|22717|5|Briefly described|P4, Fig3 P18||Archean|||||||07-NOV-08
27160|Gorge Creek Group|22727|6|Mentioned|p635,6,8||Archean|||||||07-NOV-08
27160|Gorge Creek Group|23128|5|Briefly described|p372|||||||||
27160|Gorge Creek Group|23134|5|Briefly described|p288|||||||||
27160|Gorge Creek Group|23206|6|Mentioned|Fig.1|||||||||
27160|Gorge Creek Group|23244|6|Mentioned|p15|||of Pilbara Supergroup, Pilbara Craton.||||||
27160|Gorge Creek Group|23255|5|Briefly described|p46 Fig.2||Archean|||||||07-NOV-08
27160|Gorge Creek Group|23415|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup. Geological province:  Pilbara Craton.||||||07-NOV-08
27160|Gorge Creek Group|23416|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup, Pilbara Craton||||||07-NOV-08
27160|Gorge Creek Group|23484|5|Briefly described|p5|||Of Roebourne Group.||||||
27160|Gorge Creek Group|23570|5|Briefly described|p11|||Geological Province: Pilbara Craton||||||
27160|Gorge Creek Group|23583|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup. Geological Province Pilbara Craton.||||||07-NOV-08
27160|Gorge Creek Group|23585|4|Described|p12|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
27160|Gorge Creek Group|23598|6|Mentioned|p3|||Of Pilbara Supergroup. Geological Province: Pilbara Craton.||||||
27160|Gorge Creek Group|23743|6|Mentioned|p3|Archean|Archean|Of Pilbara Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
27160|Gorge Creek Group|23745|4|Described|p4|Archean|Archean|Age: 3300-3000 Ma. See also page 7 Fig 5. Of Pilbara Supergroup. Geological Province: Pilbara Block.||||||07-NOV-08
27160|Gorge Creek Group|23755|4|Described|p42|Archean|Archean|See also page 17 table 1.||||||07-NOV-08
27160|Gorge Creek Group|23757|4|Described|p10|Archean|Archean|Includes Nimingarra Iron Formation, and parts of Cundaline Formation and Cooieena Basalt. Disconformably overlain by the De Grey Group. Age: <3235 Ma (SHRIMP U-Pb zircon). Geological Province: Pilbara Craton.||||||07-NOV-08
27160|Gorge Creek Group|23783|4|Described|p16|Archean|Archean|Of Pilbara Supergroup.||||||07-NOV-08
27160|Gorge Creek Group|23784|5|Briefly described|p2|Archean|Archean|||||||07-NOV-08
27160|Gorge Creek Group|23789|4|Described|p11|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
27160|Gorge Creek Group|23793|4|Described|p17|Archean|Archean|Of Pilbara Supergroup. Geological Province: Pilbara Craton||||||07-NOV-08
27160|Gorge Creek Group|23794|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
27160|Gorge Creek Group|23807|5|Briefly described|p109||Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
27160|Gorge Creek Group|23813|5|Briefly described|p101|Archean|Archean|Basalts and dacites; chert, clastic sediments, volcanics.  Age: ca.3240Ma.  Geological Province: Pilbara Craton.  See also p91 Tb. 1.||||||07-NOV-08
27160|Gorge Creek Group|23865|5|Briefly described|p187|Archean|Archean|Geological Province: Pilbara Block.||||||07-NOV-08
27160|Gorge Creek Group|23891|5|Briefly described|p89|Archean|Archean|Of Mount Bruce Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
27160|Gorge Creek Group|23895|5|Briefly described|p884 Fig.1|||Geological Province: Pilbara Craton.||||||07-MAR-05
27160|Gorge Creek Group|23936|4|Described|p2, p13, Tb.1|Archean|Archean|Age: <3240 Ma. Geological Province: Pilbara Craton. Underlying Unit: Sulphur Springs Group (disconformably).||||||07-NOV-08
27160|Gorge Creek Group|23956|5|Briefly described|p1264|||Overlies the Sulphur Springs Group. Unconformably overlain by the De Grey and Fortescue Groups. Geological Province: Pilbara Craton.||||||
27160|Gorge Creek Group|24024|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
27160|Gorge Creek Group|24025|4|Described|p8 Tb. 1|Archean|Archean|Interpreted date: c.3235-3000Ma.   Geological Province: Pilbara Craton.||||||07-NOV-08
27160|Gorge Creek Group|24095|4|Described|p46|||Of the Pilbara Supergroup.  Overlies the Warrawoona Group; underlies the Whim Creek Group. Geological Province: Pilbara Block.||||||30-MAR-05
27160|Gorge Creek Group|24110|5|Briefly described|Plate 1|Archean|Archean|Parent: Pilbara Supergroup.  Geological Province: Pilbara Craton||||||07-NOV-08
27160|Gorge Creek Group|24166|5|Briefly described|p12|Archean|Archean|Parent: Pilbara Supergroup.||||||07-NOV-08
27160|Gorge Creek Group|24182|5|Briefly described|p93 Fig. 3.|||Geological Province: Pilbara Craton.||||||
27160|Gorge Creek Group|24184|4|Described|p702|Archean|Archean|Parent: Pilbara Supergroup. Geological Province: Pilbara Craton. Max Thickness: 3,500m||||||07-NOV-08
27160|Gorge Creek Group|24185|5|Briefly described|p737 Tb.2|Archean|Archean|Age: 3.24-3.05 Ga. Geological Province: Pilbara Craton. Includes Cleaverville Fm. according to Van Kranendonk et al (2002), but possible, although not proven, the two were deposited in two intervals.||||||07-NOV-08
27160|Gorge Creek Group|24186|4|Described|p776, 777 Fig.2|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
27160|Gorge Creek Group|24187|5|Briefly described|p776, 777 Fig.2|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
27160|Gorge Creek Group|24188|6|Mentioned|p788|Archean|Archean|Age: 3240 Ma||||||07-NOV-08
27160|Gorge Creek Group|24194|6|Mentioned|p906 Fig.6|||Geological Province: Pilbara Craton||||||
27160|Gorge Creek Group|24327|5|Briefly described|Map Legend|Archean|Archean|Includes the Cleaverville Formation.  Parent: Pilbara Supergroup.  Age: c.3020Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
27160|Gorge Creek Group|24349|5|Briefly described|Map legend|Archean|Archean|Of Pilbara Supergroup.   Includes the Cleaverville Formation.   Age: c.3020Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
27160|Gorge Creek Group|24531|4|Described|p20|Archean|Archean|Of the Pilbara Supergroup.  Conformably overlies the Sulphur Springs Group.  See also p5 Table 1, p8-9 Fig. 3.||||||07-NOV-08
27160|Gorge Creek Group|24532|5|Briefly described|Map legend|Archean|Archean|Of the Pilbara Supergroup.||||||07-NOV-08
27160|Gorge Creek Group|24533|5|Briefly described|p4|Archean|Archean|Includes the Cleaverville Formation. Geological Province: Mallina Basin.||||||07-NOV-08
27160|Gorge Creek Group|24541|5|Briefly described|p7, p11 Tb.2, p24|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
27160|Gorge Creek Group|24543|5|Briefly described|Map legend|Archean|Archean|Of the Pilbara Supergroup.  Age: c.3020Ma.||||||07-NOV-08
27160|Gorge Creek Group|24550|6|Mentioned|p30, p31 Tb. 3.1|||Unconformably overlies the Warrawoona Group. Geological Province: Pilbara Craton.||||||07-FEB-11
27160|Gorge Creek Group|24554|6|Mentioned|p4|||||||||
27160|Gorge Creek Group|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Includes: Pyramid Hill Formation, Honeyeater Basalt, Dalton Suite and the Soanesville Subgroup. Geological Province: Pilbara Craton. See also p28 Fig. 1.2.||||||07-FEB-11
27160|Gorge Creek Group|24621|5|Briefly described|p73 Fig. 3|Archean|Archean|Bedded medium-grained sandstone and shale. Unconformably overlies the Warrawoona Group.  Age: <3.24Ga.  See also p72 Fig. 2b.||||||07-NOV-08
27160|Gorge Creek Group|29853|6|Mentioned|p154|||||||||
27160|Gorge Creek Group|30363|6|Mentioned|p10|||||||||
27160|Gorge Creek Group|30485|6|Mentioned|p74|||Refers Lipple (1975)||||||
27160|Gorge Creek Group|30766|4|Described|p13|||||||||
27160|Gorge Creek Group|31308|6|Mentioned|p68|||Precambrian. Stratigraphy||||||
27160|Gorge Creek Group|31310|6|Mentioned|p53|||||||||
27160|Gorge Creek Group|31819|6|Mentioned|p80|||||||||
27160|Gorge Creek Group|31853|2|Defined|p61|Archean|Archean|||||||07-NOV-08
27160|Gorge Creek Group|32954|6|Mentioned|p187|||||||||
27160|Gorge Creek Group|34829|6|Mentioned|p67|||||||||
27160|Gorge Creek Group|35142|6|Mentioned|p421|||||||||
27160|Gorge Creek Group|35218|6|Mentioned|p1|||||||||
27160|Gorge Creek Group|35269|6|Mentioned|p297|||||||||
27160|Gorge Creek Group|35531|6|Mentioned|Fig.1|||Composite lithostratigraphic section||||||
27160|Gorge Creek Group|35681|6|Mentioned|Table 3|||||||||
27160|Gorge Creek Group|35711|4|Described|p19|||See also Table 3, stratigraphy||||||
27160|Gorge Creek Group|35726|6|Mentioned|p120|||||||||
27160|Gorge Creek Group|35949|6|Mentioned|p333|||||||||
27160|Gorge Creek Group|35969|6|Mentioned|Fig.10|||||||||
27160|Gorge Creek Group|36257|6|Mentioned|Fig.2.1|||||||||
27160|Gorge Creek Group|36551|6|Mentioned|p55|||||||||
27160|Gorge Creek Group|37299|6|Mentioned|Fig.1|||||||||
27160|Gorge Creek Group|37633|4|Described|p12|||See also Plate 1||||||
27160|Gorge Creek Group|37899|6|Mentioned|Fig.2|||||||||
27160|Gorge Creek Group|38242|5|Briefly described|p200|||||||||
27160|Gorge Creek Group|38258|5|Briefly described|p1231|||||||||
27160|Gorge Creek Group|38481|6|Mentioned|p264|||||||||
27160|Gorge Creek Group|38498|6|Mentioned|Fig.1|||||||||
27160|Gorge Creek Group|38507|5|Briefly described|p236|||||||||
27160|Gorge Creek Group|38544|6|Mentioned|p289|||||||||
27160|Gorge Creek Group|38624|6|Mentioned|p240|||||||||
27160|Gorge Creek Group|38742|6|Mentioned|Fig.7|||||||||
27160|Gorge Creek Group|39310|6|Mentioned|p26|||||||||
27160|Gorge Creek Group|39328|6|Mentioned|p475|||||||||
27160|Gorge Creek Group|39426|6|Mentioned|p3|||||||||
27160|Gorge Creek Group|39444|6|Mentioned|p6|||||||||
27160|Gorge Creek Group|39580|4|Described|p290|||||||||
27160|Gorge Creek Group|39672|6|Mentioned|Fig.2|||||||||
27160|Gorge Creek Group|39697|3|Fully described|p96|||||||||
27160|Gorge Creek Group|39837|6|Mentioned|p260|||||||||
27160|Gorge Creek Group|40596|6|Mentioned|p65|||||||||
27160|Gorge Creek Group|40661|6|Mentioned|p90|||||||||
27160|Gorge Creek Group|41028|5|Briefly described|p227|||||||||
27160|Gorge Creek Group|41073|6|Mentioned|p200|||||||||
27160|Gorge Creek Group|41250|5|Briefly described|p30|||||||||
27160|Gorge Creek Group|41252|5|Briefly described|p49|||||||||
27160|Gorge Creek Group|41349|6|Mentioned|p4|||||||||
27160|Gorge Creek Group|41350|6|Mentioned|Fig.1|||||||||
27160|Gorge Creek Group|41351|6|Mentioned|Fig.2|||||||||
27160|Gorge Creek Group|41353|6|Mentioned|p59|||||||||
27160|Gorge Creek Group|41354|5|Briefly described|p89|||||||||
27160|Gorge Creek Group|41355|6|Mentioned|p111|||||||||
27160|Gorge Creek Group|41357|6|Mentioned|Fig.1|||||||||
27160|Gorge Creek Group|41358|6|Mentioned|Fig.1|||||||||
27160|Gorge Creek Group|41561|6|Mentioned|Fig.1 p536|||||||||
27160|Gorge Creek Group|41594|6|Mentioned|p70|||||||||
27160|Gorge Creek Group|41624|6|Mentioned|p43|||||||||
27160|Gorge Creek Group|41635|4|Described|p19|||||||||
27160|Gorge Creek Group|41678|5|Briefly described|p31|||||||||
27160|Gorge Creek Group|41767|5|Briefly described|p44|||||||||
27160|Gorge Creek Group|41768|6|Mentioned|p9|||||||||
27160|Gorge Creek Group|41851|5|Briefly described|p822|||||||||
27160|Gorge Creek Group|42231|5|Briefly described|p330|||||||||
27160|Gorge Creek Group|42260|6|Mentioned|p6|||||||||
27160|Gorge Creek Group|42352|6|Mentioned|p23|||||||||
27160|Gorge Creek Group|42730|5|Briefly described|p4|||||||||
27160|Gorge Creek Group|43052|5|Briefly described|Fig.3.8|||||||||
27160|Gorge Creek Group|43056|5|Briefly described|Map Legend|||||||||
27160|Gorge Creek Group|43562|6|Mentioned|Fig.3, p576|||||||||
27160|Gorge Creek Group|43595|6|Mentioned|Fig.2-47,211|||||||||
27160|Gorge Creek Group|43644|6|Mentioned|p593|||||||||
27160|Gorge Creek Group|43698|6|Mentioned|p3||Archean|Late Archaean||||||07-NOV-08
27160|Gorge Creek Group|43769|6|Mentioned|p855|||Age: approx.3.3 Ga||||||
27160|Gorge Creek Group|43779|3|Fully described|p1-21||Archean|Age: 3000-3400 Ma.||||||07-NOV-08
27160|Gorge Creek Group|44150|5|Briefly described|p129 Tb.2-15, p132 Figs.2-131,-132|||See also p134-140, p155. |3.3 - 3.0 Ga.|Pilbara Supergroup|Soanesville Subgroup; Mosquito Creek Formation; Honeyeater Basalt; Lalla Rookh Sandstone.|Unconformably overlies Warrawoona Group.||
27160|Gorge Creek Group|44151|6|Mentioned|p162|||||Pilbara Supergroup|Includes Mosquito Creek Formation.|||
27160|Gorge Creek Group|44152|6|Mentioned|p162, p170|||||Pilbara Supergroup|Includes Mosquito Creek Formation.|||
27160|Gorge Creek Group|44189|5|Briefly described|Map legend||Archean|||||||07-NOV-08
27160|Gorge Creek Group|44229|5|Briefly described|Map Legend|Archean|Archean|Of the Pilbara Supergroup.  Includes the Nimingarra Iron, Cundaline and Coonieena Formations.||||||07-NOV-08
27160|Gorge Creek Group|46319|5|Briefly described|p3|Archean|Archean|Of Pilbara Supergroup.  Geological Province: Pilbara Craton.||||||07-NOV-08
27160|Gorge Creek Group|46922|6|Mentioned|p259|||Trace element analysis.||||||
27160|Gorge Creek Group|50189|4|Described|p16|Archean|Archean|Of the Pilbara Supergroup. Formerly "Gorge Creek Formation", previously included in De Grey Group. Unconformably overlies Muccan Granitoid Complex, Warrawoona Group. Disconformably overlain by the De Gray Group. Age: <3240Ma.||||||07-NOV-08
27160|Gorge Creek Group|50302|5|Briefly described|Map Legend|Archean|Archean|Of the Pilbara Supergroup. Includes Cleaverville, Nimingarra Iron and Corboy Formations.  Geological Province: Pilbara Craton.||||||07-NOV-08
27160|Gorge Creek Group|50370|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup. Geological Province: Pilbara Craton||||||07-NOV-08
27160|Gorge Creek Group|50379|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
27160|Gorge Creek Group|50381|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
27160|Gorge Creek Group|50382|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton. Age: c. 3020 Ma||||||07-NOV-08
27160|Gorge Creek Group|50383|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup. Geological Province: Pilbara Craton||||||07-NOV-08
27160|Gorge Creek Group|50423|5|Briefly described|p215, Fig.1, p216||Archean|Clastic Sediments. East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
27160|Gorge Creek Group|50427|4|Described|p182 Fig.5|Archean|Archean|Age: <3230 Ma. Unconformably and conformably overlies Sulphur Springs Group, unconformably overlies Coonterunah and Warrawoona Groups. Unconformably overlain by De Grey Group. BIF, basal quartzite, conglomerate, shale and siltstone. Of Pilbara Supergroup.||||||07-NOV-08
27160|Gorge Creek Group|50430|4|Described|p158 Tb.1||Archean|Deposited 3235-3020? Ma. Clastic sediments including banded iron formations up to 1km thick. In East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
27160|Gorge Creek Group|50435|6|Mentioned|p2.1|||Geological Province: Kimberley Block. Intruded by Bridget Suite.||||||
27160|Gorge Creek Group|50544|3|Fully described|p31-32, p10|Archean|Archean|Of the Pilbara Supergroup.  Age: c.3.24-2.94Ma.  Unconformably overlies Warrawoona Gp, and the Warrawagine and Muccan Granitoid Complexes; disconformably underlies Cattle Well Fm; unconformably underlies Eel Creek and Callawa Fms.  see also p18.||||||07-NOV-08
27160|Gorge Creek Group|50555|5|Briefly described|Map legend|Archean|Archean|Of the Pilbara Supergroup.  Includes the Cundaline and Nimingarra Iron Formations, and the Coonieena Basalt.  Geological Province: Pilbara Craton.||||||07-NOV-08
27160|Gorge Creek Group|60112|5|Briefly described|p106, p107-109 Figs.1,2, p115-117, |||Displays syn-depositional extensional faulting.|<3240 Ma (Hickman, 1983).|||Of the Pilbara Supergroup.|Mostly metasedimentary rocks, contain banded iron-formation (BIF)|
27160|Gorge Creek Group|60429|4|Described|p6 Fig. 3, p16|Archean|Archean|Includes Nimingarra Iron Formation. Unconformably overlies Warrawagine Granitoid Complex.  Age: <3240Ma. Geological Province: Pilbara Craton. See also p8 Fig. 4.||||||07-FEB-11
27160|Gorge Creek Group|60636|5|Briefly described|p35-36 Fig. 3.2|||Includes Wyman and Nimingarra Iron Formations. Overlies the Warrawoona Group.||||||07-FEB-11
27160|Gorge Creek Group|61111|5|Briefly described|p96 Fig.2, p102, 103, 108||Paleoarchean|Detailed chemical analyses.|c.3240 Ma. |||||
27160|Gorge Creek Group|61205|4|Described|p548 Fig. 1|||Geological Province: Pilbara Craton. Overlain by De Grey and Fortescue Group; underlain by Sulphur Springs Group. Iron formation and turbidites.||||||31-MAY-07
27160|Gorge Creek Group|61252|6|Mentioned|p65|||||||||
27160|Gorge Creek Group|61253|5|Briefly described|p51, p50 Fig. 1, p52 Fig. 2|Archean|Archean|Of Pilbara Supergroup. Redefined as: Tank Pool Qtzt , Nimingarra Iron, Pincunah Hill, Corboy and Paddy Market Fms, Honeyeater Basalt and Pyramid Hill Fm. Overlies Sulphur Springs Supergp; overlain by either De Grey or Mt Bruce Supergroups. Age: <3.27Ga.||||||07-NOV-08
27160|Gorge Creek Group|61264|6|Mentioned|p62|Archean|Archean|Age: c3240Ma.||||||07-NOV-08
27160|Gorge Creek Group|61266|4|Described|p55|Archean|Archean|Overlies the Sulphur Springs Group. Geological Province: Pilbara Craton. See also p58 Tb.1||||||07-NOV-08
27160|Gorge Creek Group|61579|5|Briefly described|p58 Fig. 2|Archean|Archean|Unconformably overlain by De Grey Group; unconformably overlies Sulphur Springs Group. ||||||07-NOV-08
27160|Gorge Creek Group|62427|5|Briefly described|p2, p3 Fig.2, p4, p6. |||Coppin Gap Greenstone Belt. A silicified banded sandstone was dated at 3459 +/- 4 Ma (detrital zircons).|||Includes Nimingarra Formation.|Unconformably overlies the Warrawoona Group.|Sandstone, chert, silicified basalt and minor felsic volcanic rock; banded iron formation, banded and ferruginous chert.|
27160|Gorge Creek Group|63110|6|Mentioned|p1125 Fig. 5|||Consists of turbidites.||||||11-JUN-08
27160|Gorge Creek Group|63245|5|Briefly described|p4 Fig. 1|Archean|Archean|Age: c.3240Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
27160|Gorge Creek Group|63372|5|Briefly described|Map Legend|Archean|Archean|Of the Pilbara Supergroup. Geological Province: East Pilbara Granite-Greenstone Terrane. Age <3016Ma.||||||07-NOV-08
27160|Gorge Creek Group|63417|5|Briefly described|Map legend|Archean|Archean|Of De Grey Supergroup.  Includes Farrel Quartzite and Cleaverville Formation and unassigned metamoprhosed sandstone, siltstone, conglomerate. Age: c. 3020Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
27160|Gorge Creek Group|63420|5|Briefly described|Map legend|Archean|Archean|Of the De Grey Supergroup. Includes Farrel Quartzite and Cleaverville Formation.  Age: c.3020Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
27160|Gorge Creek Group|63441|4|Described|p5 Tb. 1, p26|Archean|Archean|Of the De Grey Supergroup. Comprises Farrel Quartzite and Cleaverville Groups and Cundaline Formation. Age: 3020Ma. Geological province: Gorge Creek Basin, Pilbara Craton.||||||07-FEB-11
27160|Gorge Creek Group|63538|4|Described|p2 Fig. 1, p6 Fig. 3|Archean|Archean|Includes Cleaverville Formation, Cundaline Formation and Farrel Quartzite. Age: 3020 Ma. Geological Province: Pilbara Craton. Sedimentary rocks.||||||19-APR-13
27160|Gorge Creek Group|63649|5|Briefly described|p201|Archean|Archean|Of the Pilbara Supergroup. Age: ca.3.23 - 3.0Ga. Geological Province: Pilbara Craton.||||||07-FEB-11
27160|Gorge Creek Group|63854|5|Briefly described|p228, p229 Fig.2  |Paleoarchean|Paleoarchean|East Pilbara Terrane.|ca. 3240 Ma|||||
27160|Gorge Creek Group|63866|5|Briefly described|p144|||||||Intruded by the Bridget Suite.||
27160|Gorge Creek Group|64174|5|Briefly described|Map legend|Archean|Archean|Of De Grey Supergroup. Includes Cleaverville Formation. Geological province: Gorge Creek Basin, Pilbara Craton.||||||07-NOV-08
27160|Gorge Creek Group|64326|6|Mentioned|p72|Archean|Archean|||||||07-FEB-11
27160|Gorge Creek Group|64327|5|Briefly described|p61|Archean|Archean|Unconformably overlies Budjan Creek Formation. Dominantly clastic rocks. Age: <3235Ma.||||||07-NOV-08
27160|Gorge Creek Group|64328|4|Described|p54, p58|Archean|Archean|Includes Soanesville Subgroup and Honeyeater Basalt. Overlies Budjan Creek Formation with low angle unconformity. Age: 3240-2940ma.||||||07-FEB-11
27160|Gorge Creek Group|64384|5|Briefly described|p26 Tb. 3|Archean|Archean|Of the Pilbara Supergroup. Includes Corboy Formation, Charteris Basalt, Cleaverville Formation, Honeyeater Basalt, Lalla Rookh Sandstone and Mosquito Creek Formation.||||||07-FEB-11
27160|Gorge Creek Group|64580|4|Described|map legend|Mesoarchean|Mesoarchean|Of De Grey Supergroup. Banded iron formation, chert, siliciclastic sedimentary rocks, and mafic volcanic rocks; metamorphosed.||||||09-DEC-08
27160|Gorge Creek Group|64621|5|Briefly described|Map legend|Archean|Archean|Of De Grey Supergroup. Includes Farrel Quartzite and Cleaverville Formation, and unassigned rocks of sandstone, siltstone, conglomerate, with minor siltstone/shale, metamorphosed.||||||07-NOV-08
27160|Gorge Creek Group|64628|6|Mentioned|p170, p171 Fig.1.|||With the Warrawoona Group, forms the east-west striking Coppin Gap greenstone belt, northeast of Marble Bar.|||Includes Nimingarra Iron Formation.|||
27160|Gorge Creek Group|64632|5|Briefly described|p201 Fig.1, p203, 207|Mesoarchean|Mesoarchean||3020 Ma|Of the De Grey Supergroup.|Includes Cleaverville Formation|Unconformably overlain by the Whim Creek Group.||
27160|Gorge Creek Group|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Pilbara Supergroup. Includes Corboy Formation and Paddy Market Formation. Geological Province: Pilbara Craton.||||||07-FEB-11
27160|Gorge Creek Group|64654|5|Briefly described|Map Legend|Archaean|Archaean|Undivided banded iron-formation, inferred from aeromagnetic data. Geological Province: Pilbara Craton.||||||17-NOV-08
27160|Gorge Creek Group|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Pilbara Supergroup. Includes Pincunah Hill Formation. Geological Province: Pilbara Craton.||||||
27160|Gorge Creek Group|64747|6|Mentioned|p94 fig 1|Paleoarchean|Paleoarchean||c.3240 Ma.|||||
27160|Gorge Creek Group|64936|5|Briefly described|map legend|Archean|Archean|Of Pilbara Supergroup. Includes Soanesville Subgroup. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
27160|Gorge Creek Group|65008|5|Briefly described|p2, p5, p7, p8 Fig.5, p11-16, p22, p41|Mesoarchean|Mesoarchean||3200-2940 Ma|Of the Pilbara Supergroup|Includes Paddy Market Formation and Corboy Formation.|Unconformably overlain by De Grey Group and Mount Roe Basalt. Unconformably underlain by Wyman and Budjan Creek Formations, Charteris Basalt, Warrawoona and Sulphur Springs Groups (disconformably).|Dominantly sedimentary.|
27160|Gorge Creek Group|65415|6|Mentioned|p120 Fig.2.|Archean|Archean||c.3.32 - 3.2 Ma.|Unit in Pilbara Supergroup.||Unconformably overlies Wyman Formation. Is overlain unconformably by De Grey Group.||
27160|Gorge Creek Group|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||Of Pilbara Supergroup. |Includes Nimingarra Iron Formation and Corboy Formation.||Undivided: metamorphosed sedimentary and volcanic rocks (Section only).|
27160|Gorge Creek Group|65727|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Gorge Creek Basin, Pilbara Craton.|<3235 Ma.|Of De Grey Supergroup. |Includes Farrel Quartzite and Cleaverville Formation.||Undivided: banded iron-formation and siliciclastic sedimentary rock; metamorphosed (Section only).|
27160|Gorge Creek Group|65825|6|Mentioned|p5. |Archean|Archean|||Unit in Pilbara Supergroup according to Van Kranendonk et al. (2001, 2002).||||
27160|Gorge Creek Group|65827|3|Fully described|p1, p8, p12 Tb.3, p16, p21-22, p28, p31|Mesoarchean|Mesoarchean|Of De Grey Supergroup (Van Kranendonk et al. 2006). Includes Farrel Quartzite and Cleaverville Formation. Formerly of Pilbara Supergroup where it included Corboy Formation and Nimingarra Iron Formation. Faulted against Zulu Granodiorite; unconformably overlies Pilbara Supergroup, Warrawoona Group, Kelly Group, Wyman Formation, Charteris Basalt; underlies Fortescue Group. Deposition <3235-2980 Ma; folding, uplift and erosion c.2950 Ma. Epiclastic material mostly derived from elevated granitic domes, and banded iron-formation.||||||
27160|Gorge Creek Group|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Gorge Creek Basin, De Grey Superbasin. Unit of De Grey Supergroup. Includes Farrel Quartzite, Cleaverville Formation, and an unnamed unit consisting of metamorphosed banded iron-formation and siliciclastic sedimentary rock.||||||
27160|Gorge Creek Group|66118|5|Briefly described|p146-148, p153 Fig.7, p158-159|||Pilbara Craton.|3020 Ma|Stratigraphically lowest in De Grey Supergroup||Is unconformably overlain by Whim Creek Group.|Chert and iron formation; felsic volcaniclastic sandstone.|
27160|Gorge Creek Group|66122|5|Briefly described|p74|Archean|Archean||3.02 Ga.|De Grey Supergroup.|Farrel Quartzite, Cleaverville Formation.|Unconformably overlies Pilbara Supergroup.||
27160|Gorge Creek Group|66217|4|Described|p1, p6 Table 1, p9, p17, pp38-41, p60.|Mesoarchean|Mesoarchean|Gorge Creek Basin, West Pilbara Superterrane and East Pilbara Terrane, Pilbara Craton. Deposited during orogenic relaxation; thickness to c.1900 m. Experienced syn-depositional growth faulting and post-depositional tilting. Hosts local gossanous Cu-Au-Ag mineralisation in western Gorge Range.|3020 Ma.|Basal unit in De Grey Supergroup.|Includes Farrel Quartzite at the base, Cleaverville Formation, Corboy Formation.|Unconformably overlies Talga Talga and Coongan Subgroups. Is unconformably overlain by Whim Creek and Croydon Groups.||10-JUN-20
27160|Gorge Creek Group|66745|5|Briefly described|p50 Fig.1, p53|Mesoarchean|Mesoarchean|Soanesville Group removed from this unit in 2006. Moved from Pilbara Supergroup to De Grey Supergroup in 2006.|3050-3020 Ma.|Unit in De Grey Supergroup.||||12-OCT-15
27160|Gorge Creek Group|67130|6|Mentioned|p13, p14 fig 9|Mesoarchean|Mesoarchean||3020 Ma- 2970 Ma|De Grey Supergroup||Overlies Whundo Group, overlain by Whim Creek Group,  De Grey Supergroup||
27160|Gorge Creek Group|67197|5|Briefly described|p2, p5, p9, p14, p19, p22, p29, p33-34|Paleoarchean|Paleoarchean|See also p36. De Grey Superbasin.|c.3020 Ma.|De Grey Supergroup.|Farrel Quartzite, Cleaverville Formation.|Overlies Soanesville Group. Is overlain unconformably by Croydon Group.||
27160|Gorge Creek Group|67201|4|Described|p7, p12-13, p15-17, p20-22, see comments|Archean|Archean|Unconformable over West Pilbara Superterrane and East Pilbara Terrane. Comprises all of Gorge Creek Basin, De Grey Superbasin. Age range also stated elsewhere as 3050-3015 Ma. Page location continued: p24, p26-27, p64, p69.|3050-3020 Ma|Base of De Grey Supergroup|East Pilbara: basal Cleaverville Formation, central Farrel Quartzite, uppermost Cundaline Formation. West Pilbara: Cleaverville Formation only.|Overlies Pilbara Supergroup and Soanesville Group unconformably; Whundo Group and Regal Formation nonconformably. Is unconformably overlain by Whim Creek Group.||22-NOV-16
27160|Gorge Creek Group|67269|6|Mentioned|p5|Paleoarchean|Paleoarchean||||Dalton Suite; Cleaverville Formation.|||
27160|Gorge Creek Group|67270|6|Mentioned|p4|||||||||
27160|Gorge Creek Group|67668|6|Mentioned|Fig. 2; p. 154-5, Tb.1.||Mesoarchean|East Pilbara Terrane, Pilbara Craton.|c.3020 Ma.|De Grey Supergroup|Includes Farrel Quartzite.|Unconformably overlies the Pilbara Supergroup.||
27160|Gorge Creek Group|68035|5|Briefly described|p290, 289, p286 Fig 3, p290 Fig 5|Mesoarchean|Mesoarchean|Gorge Creek Basin, De Grey Superbasin. Deposition was initially in shallow-water, and included evaporite and fluviatile deposits (Sugitani et al., 1998).|3050 - 3020 Ma||Includes Cleaverville Formation.||Basal conglomerate and sandstone overlain by a 1,000 m-thick unit of BIF, chert, and black shale.|
27160|Gorge Creek Group|68280|6|Mentioned|p3|Mesoarchean|Mesoarchean||3050-3020 Ma|||||
27160|Gorge Creek Group|68281|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Gorge Creek Basin, De Grey Superbasin, Pilbara Craton.||Of the De Grey Supergroup.|Includes Cleaverville Formation, Farrel Quartzite.|||23-SEP-13
27160|Gorge Creek Group|68283|5|Briefly described|Map Legend|Archean|Archean|Gorge Creek Basin.||Of the De Grey Supergroup.|Includes Cleaverville Formation, Farrel Quartzite.|||23-SEP-13
27160|Gorge Creek Group|68284|6|Mentioned|p4|||Crops out in the Marble Bar-Nullagine area, East Pilbara Terrane.|3050-3020 Ma.|||||
27160|Gorge Creek Group|69012|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Gorge Creek Basin.|3022-3016 Ma|Of the De Grey Supergroup.|Includes Cleaverville Formation and Farrel Quartzite.||Includes pebble conglomerate, ferruginous shale, banded iron-formation, ferruginous chert, local banded quartz-magnetite-grunerite rock; all metamorphosed.|29-APR-14
27160|Gorge Creek Group|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Gorge Creek Basin. Age constrained by the age of the Cleaverville Formation.||Of the De Grey Supergroup.|Includes the Cleaverville Formation and Farrel Quartzite.|||14-NOV-16
27160|Gorge Creek Group|69015|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Gorge Creek Basin, De Grey Superbasin.||Of the De Grey Supergroup.|Includes the Cleaverville Formation and the Farrel Quartzite.||Includes banded iron-formation and ferruginous chert; black shale with minor chert and banded iron-formation; sandstone and minor interbedded conglomerate.|02-MAY-14
27160|Gorge Creek Group|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|Age derived from samples of meta quartz arenite and quartzite (168990.1.pdf, 168997.1.pdf) - where it is interpreted as the age of igneous crystallisation of a volcanic component of the sedimentary protolith to the quartzite.|3459 +/- 7 Ma, 3410 +/- 6 Ma (SHRIMP)|De Grey Supergroup|Includes Cundaline Formation, Cleaverville Formation, Farrek Quartzite,||Dolerite; in sills; metamorphosed. Sandstone, siltstone, conglomerate, shale, chert, and banded iron-formation; metamorphosed.|
27160|Gorge Creek Group|69185|4|Described|GEOL_LUT_CSV files|||Geological Province: Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.||Unit of De Grey Supergroup.|Includes Cleaverville Formation, Paddy Market Formation, Nimingarra Iron Formation, Pincunah Hill Iron Formation.||Banded iron-formation, metamorphosed sandstone, siltstone, and shale; graded bedding and local cross-bedding; includes metamorphosed turbidite deposits|
27160|Gorge Creek Group|69300|5|Briefly described|map legend|Archean|Archean|West Pilbara Granite-Greenstone Terrane||Pilbara Supergroup|Cleaverville Formation|||
27160|Gorge Creek Group|69301|4|Described|p5-6, p9 Tb.1, p14-15, p20 Tb.2, p22|||Pilbara Craton. West Pilbara Superterrane and East Pilbara Terrane. Entire Gorge Creek Basin. Thickness: up to 2000 m.|3.05-3.02 Ga|Base of oldest group in De Grey Supergroup|Cleaverville Formation, Cundaline Formation, Farrel Quartzite|Angular unconformity upon Pilbara Supergroup, Soanesville Group, and deeply eroded Paleoarchean granitic rocks. Unconformably overlies (without angular discordance) Regal Formation and Whundo Group.|Sandstone, shale, and BIF.|
27160|Gorge Creek Group|69548|6|Mentioned|p2|||Pilbara region.||||Unconformably overlies Sulphur Springs Group.|Breccia, sandstone, wacke, mudrock, gabbro, BIF, mafic volcanic rocks.|
27160|Gorge Creek Group|69569|6|Mentioned|p285 Fig.1|||East Pilbara Terrane.||||||
27160|Gorge Creek Group|69590|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton. Of Gorge Creek Basin, De Grey Superbasin. Events: North Pilbara Orogeny. Sample GSWA 168990 (quartzite) yielded an interpreted maximum depositional age of 3496+\-4 Ma for the sandstone, and also represents igneous crystallisation age of the volcanigenic components of the sandstone (weighted mean 207pb/206Pb). Sample GSWA 168997 (quartzite) yielded an interpreted maximum depositional age of 3410+\-6 Ma for the sandstone precursor, and also represents igneous crystallisation age of the volcanigenic components of the sandstone (weighted mean 207pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeol_lut.csv.|3066-3016 Ma (inferred)|Unit of De Grey Supergroup.|Includes Cleaverville Formation, Cundaline Formation, Farrel Quartzite.||Sandstone, siltstone, conglomerate, shale, chert, and banded iron-formation; metamorphosed; dolerite sills.|16-JAN-23
27160|Gorge Creek Group|70022|5|Briefly described|p114-115|||De Grey Superbasin, Pilbara Craton.|3050-3015 Ma.|De Grey Supergroup.|Cleaverville, Cundaline Formations; Farrel Quartzite.|Unconformably overlies Soanesville Group. Is overlain unconformably by Croydon Group.||
27160|Gorge Creek Group|70507|6|Mentioned|p431|Archean|Archean|Geological province: Pilbara Craton.||||||
27160|Gorge Creek Group|70775|5|Briefly described|iii, p11, p12-p13, p15, p18, p38|||Gorge Creek Basin. Deposited in an extensional continental basin following the Prinsep Orogeny. In 1980 this group contained rocks belonging to both the current Soanesville Group and the current Gorge Creek Group in addition to parts of the Croydon Group. See also  p40-p41, p43-p47, p52, p54-p55, p57, p62, p68, p73, p100.|c. 3020 Ma|De Grey Supergroup|Includes the Farrel Quartzite, Cleaverville Formation and the Cundaline Formation.|Unconformably overlies the Whundo Group. Unconformably overlain by the Whim Creek Group. Overlain by the Croydon Group and the Lalla Rookh Sandstone. Intruded by the Orpheus Supersuite.||
27160|Gorge Creek Group|70834|6|Mentioned|p298|Paleoarchean|Paleoarchean|Marble Bar greenstone belt, Pilbara Craton.||||Unconformably overlies Euro Basalt.|Siliciclastics, BIF.|
27160|Gorge Creek Group|70884|5|Briefly described|p123|Mesoarchean|Mesoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Of De Grey Superbasin.|3.02-3.01 Ga|||||
27160|Gorge Creek Group|71041|6|Mentioned|p43, 45 fig 2, p47 fig 4|||In De Grey Superbasin.|||Includes the Cleaverville Formation.|Overlies the Soanesville Group. Overlain by the Croydon Group.||10-NOV-17
27160|Gorge Creek Group|71137|6|Mentioned|p2-5, 12|Archean|Archean|Deposited on basement with considerable vertical relief. Up to 1900m thick.|||Cleaverville Formation, Farrel Quartzite.|Is overlain unconformably by the Croydon Group.||
27160|Gorge Creek Group|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||chert, banded iron formation, sandstone, conglomerate|
27160|Gorge Creek Group|71808|6|Mentioned|p97|||||||||
27160|Gorge Creek Group|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Gorge Creek Basin.|Max age ~3066 Ma, min age 3015+/-5 Ma.|De Grey Supergroup|Includes Cundaline Formation, Cleaverville Formation, Farrel Quartzite.||Banded iron-formation and siliciclastic rocks.|
27160|Gorge Creek Group|72251|5|Briefly described|p52,54|Mesoarchean|Mesoarchean|Geological province: East Pilbara Terrane and West Pilbara Superterrane, Pilbara Craton. Of De Grey Superbasin.|3050-3015 Ma|Uunit of De Grey Supergroup.|Includes Cundaline and Cleaverville formations and Farrel Quartzite.|Overlain unconformably by Whim Creek and Croydon groups. Underlain unconformably by Whundo or Soanesville groups.||
27160|Gorge Creek Group|72668|4|Described|p2-4, p12-14, p16, p19-22, p25, p28, p29|||West Pilbara Superterrane and Karratha terrane. Oldest and most widespread member of the De Grey Supergroup. Overlies unconformably older tectono-stratigraphic terranes of the WPS. Contains detrital zircons dated at 3195 Ma in tuffs immediately above the Regal Formation.|c. 3020 Ma|De Grey Supergroup|Includes the Cleaverville Formation, Budjan Creek Formation, Farrel Quartzite, and the Cundaline Formation.|Unconformably overlain by the Whim Creek Group and the Fortescue Group. Unconformably overlies the Pilbara Supergroup.|Clastic sedim entary rocks, felsic tuffs, porphyries and banded iron formation.|13-JAN-22
27160|Gorge Creek Group|73598|6|Mentioned|p1212|Mesoarchean|Mesoarchean|East Pilbara Terrane.||De Grey Supergroup.|Farrel Quartzite; Cleaverville, Cundaline Formations.|Unconformably overlies Soanesville Group. Is overlain unconformably by Croydon Group.||
78983|Gossan Hill Formation|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton.|c.2963-c.2947 Ma.|Murchison Supergroup.|Gossan Valley, Golden Grove, Scuddles, Minjar Members.||Felsic volcanic and volcaniclastic rocks, rhyolitic to dacitic in composition; locally with economic massive sulfide mineralisation; metamorphosed.|
78983|Gossan Hill Formation|70796|4|Described|100k_geologyp_lut.csv|Mesoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. See also 100K_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 155879.1.pdf, 203702.1.pdf, 203703.1.pdf, 203704.1.pdf, 211102.1.pdf, Badja100_2240_stratig.pdf. Numerous additional lithologies are discussed. Coeval with rocks of the Bunnawarra Suite.|ca 2963 to 2947 Ma (inferred)|Murchison Supergroup|Includes the Minjar Member, Scuddles Member, Golden Grove Member and the Gossan Valley Member.|Intruded by the Gnows Nest Granodiorite.|Felsic volcanic and volcaniclastic rocks, rhyolitic to dacitic in composition; locally with economic massive sulphide mineralization; metamorphosed.|
78983|Gossan Hill Formation|70830|5|Briefly described|p7, p9, p58|Mesoarchean|Mesoarchean|Ages are derived from Yeats et al, 1996 and Wang et al, 1998.|c. 2960 Ma|Murchison Supergroup|||Volcano-sedimentary rocks.|
78983|Gossan Hill Formation|71269|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.|2963-2947 Ma|Unit of Murchison Supergroup.|Includes Golden Grove Member, Gossan Valley Member, Minjar Member, Scuddles Member.|Coeval with Thunderlarra Supersuite/Bunnawarra Suite. Intruded by Gnows Nest Granodiorite.|Felsic volcanic and volcaniclastic rocks, rhyolitic to dacitic in composition; locally with economic massive sulphide mineralization; metamorphosed.|
78983|Gossan Hill Formation|71272|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. The four Members are mapped separately.||Murchison Supergroup.|Gossan Valley, Golden Grove, Scuddles, Minjar Members.|||
78983|Gossan Hill Formation|73023|5|Briefly described|p3|Mesoarchaean|Mesoarchaean|Surrounds the Yalgoo Dome.|2963-2958 Ma.|||Is overlain unconformably by the Norie and Polelle Groups.|Greenstone sequences.|
78984|Gossan Valley Member|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton.|c.2959 Ma.|Gossan Hill Formation.|||Quartz-porphyritic rhyolite and felsic volcaniclastic rocks; metamorphosed.|
78984|Gossan Valley Member|70796|5|Briefly described|100k_geologyp_lut.csv|Mesoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. See also 100K_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 203702.1.pdf, Badja100_2240_stratig.pdf. Numerous additional lithologies are discussed.|2959 +/ 5 Ma (isotopic)|Gossan Hill Formation||Overlain by the Scuddles Member.|Quartzporphyritic rhyolite and felsic volcaniclastic rocks; metamorphosed|
78984|Gossan Valley Member|71269|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). Wingate et al. 92015b0 dated a metarhyolite sample intersected in drillhole G12/501 at 2959+\-5 Ma. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv.|2959+\-5 Ma (isotopic)|Unit of Gossan Hill Formation.||Overlain by Scuddles Member.|Felsic volcanic and volcaniclastic rocks, rhyolitic to dacitic in composition; locally with economic massive sulphide mineralization; metamorphosed|
78984|Gossan Valley Member|71272|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c.2959 Ma.|Gossan Hill Formation.|||Quartz-porphyritic rhyolite and felsic volcaniclastic rocks; metamorphosed.|
80208|Government Dam member|71166|5|Briefly described|p23|||[An informal, probable company name from the Kanowna gold camp]|||||Feldspathic volcaniclastic sandstone.|
80208|Government Dam member|73391|4|Described|p132, 148-153, 174, 182-183, 194, 196|||See also p198, 225, 244, 444. Exposed at Kanowna Government Dam, Kanowna district. Estimated thickness is 1100m. Appears as Government Dam sandstone on p150. Described in some detail: outcrop map, photographs.|2661 +/- 11 Ma (MDA: Squire, 2007).|Black Flag Formation.||Unconformably overlies Grave Dam and Golden Valley members (Upper Black Flag Group) and Kanowna and Ballarat members. Is overlain unconformably by Panglo conglomerate.|A deformed pair of sequences: soft-sediment siltstone horizons, and an upper sequence of normally-graded channelised conglomerate horizons gradational into sandstone-siltstone. Graded beds.|
80976|Granites-Tanami Orogen granitic unit 80976|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. Age inferred.|||||Biotite monzogranite.|
80978|Granites-Tanami Orogen metamorphosed igneous felsic unit 80978|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Granites-Tanami Orogen. Age inferred.|||||Foliated biotite-muscovite-quartz--plagioclase-K-feldspar orthogneiss with thin leucocratic quartz-feldspar interlayers.|
31107|Granitoid Gneiss|43478|3|Fully described|p28|||'informal name'||||||
34939|Granny Smith Granodiorite|22855|6|Mentioned|p426|||||||||
34939|Granny Smith Granodiorite|23786|5|Briefly described|p34|||Geological Province: Yilgarn Craton.||||||
34939|Granny Smith Granodiorite|24196|5|Briefly described|p27, p49, p73|Archean|Archean|Age: 2665 +/- 4 Ma (Hill et al., 1992)||||||07-NOV-08
34939|Granny Smith Granodiorite|64775|6|Mentioned|p16-1|||||||||
34939|Granny Smith Granodiorite|66880|6|Mentioned|p19, p24. |Archean|Archean|This age may be the age of zircon xenocrysts derived from the turbidites intruded by the granodiorite.|2665 +/- 5 Ma.|||||
34939|Granny Smith Granodiorite|66937|6|Mentioned|pp169-170.|Archean|Archean|||||||
34939|Granny Smith Granodiorite|70271|6|Mentioned|p556|||Association with gold mineralisation is interpreted to be a result of structural favorability rather than due to orthomagmatic processes. See also references to Granny Smith granodiorite (p541, 554).||||||
34939|Granny Smith Granodiorite|71166|6|Mentioned|p49, p50, p54, p111, p114, p115, p163|||Hosts the Granny Smith gold deposit on its eastern margin where it contacts metasedimentary country rock. Carbon isotope anomalies and its relation to gold mineralisation is discussed briefly. ||||||
76189|Grass Flat Gabbro|67129|5|Briefly described|p55|Archean|Archean|Southern Cross Domain, Youanmi Terrane.|2796 +/- 6 Ma.|||||
76189|Grass Flat Gabbro|67888|6|Mentioned|p61|Archean|Archean||2796 +/-6 Ma||||Leucogabbro.|
76189|Grass Flat Gabbro|68108|6|Mentioned|p652|Neoarchean|Neoarchean||2796 +/- 6 Ma (Wingate et al. 2011)|||||
76189|Grass Flat Gabbro|68109|5|Briefly described|p659, p667|Neoarchean|Mesoarchean|Southern Youanmi Terrane. Formed due to mafic-ultramafic magmatic episodes after 2820 Ma. |c.2800 Ma U-Pb zircon (Wingate et al. 2011).||||Mafic intrusion.|03-NOV-14
76189|Grass Flat Gabbro|69404|5|Briefly described|p7|Neoarchean|Neoarchean|Southern Cross Domain, Marda-Diemals greenstone belt.|c. 2796 Ma||||Gabbroic sill.|
76189|Grass Flat Gabbro|69617|6|Mentioned|p154|||Wingate et al. (2011).||||||
76189|Grass Flat Gabbro|70156|4|Described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Youanmi Terrane events (3200-2600 Ma).|2796+\-6 Ma (isotopic)||||Gabbro; minor leucogabbro, quartz gabbro and pegmatoidal components; metamorphosed|
76189|Grass Flat Gabbro|70794|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Youanmi Terrane, Yilgarn Craton.|2796+/-6 Ma||||Gabbro; minor leucogabbro, quartz gabbro and pegmatoidal components; metamorphosed.|
76189|Grass Flat Gabbro|70796|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Younami Terrane.|2796 +/ 6 Ma (isotopic)||||Gabbro; minor leucogabbro, quartz gabbro and pegmatoidal components; metamorphosed.|
76189|Grass Flat Gabbro|70830|5|Briefly described|p27-p28|||Southern Cross Domain.||||||
76189|Grass Flat Gabbro|71168|6|Mentioned|p27|||||||||
76189|Grass Flat Gabbro|71269|4|Described|500k_interpgeop16_lut.csv|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma).|2796+\-6 Ma (isotopic)||||Gabbro; minor leucogabbro, quartz gabbro and pegmatoidal components; metamorphosed|
76189|Grass Flat Gabbro|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Youanmi Terrane.|2796+/-6 Ma.||||Gabbro; minor leucogabbro, quartz gabbro and pegmatoidal components; metamorphosed.|
76189|Grass Flat Gabbro|73596|6|Mentioned|p1170|Neoarchean|Neoarchean|Southern Cross Domain, Youanmi Terrane.|2796 +/- 6 Ma.|Polelle Group.||Intrudes Polelle Group.||
82958|Grave Dam Member|73238|5|Briefly described|p21|||Kanowna district, Eastern Goldfields Terrane.|2668 +/- 10 Ma (Tripp, 2013).|Black Flag Formation.|||Volcaniclastics.|
77865|Great Boulder Suite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2680 +/- 8 Ma (isotopic).||Includes Athena Basalt; Aberdare, Condenser, Golden Mile, Stony Hill, Three Mile Dolerites; Triumph Gabbro.|||
77865|Great Boulder Suite|71270|5|Briefly described|100k_interpgeop_lut.csv|||Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. |||Includes Aberdare Dolerite, Athena Basalt, Condenser Dolerite, Golden Mile Dolerite, Stony Hill Dolerite, Three Mile Dolerite, Triumph Gabbro.|||
29944|Greenbushes Pegmatite|23785|5|Briefly described|p8|Archean|Archean|Age: 2527Ma.  Geological Province: Yilgarn Craton.||||||07-NOV-08
29944|Greenbushes Pegmatite|23788|5|Briefly described|p2|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
29944|Greenbushes Pegmatite|43052|5|Briefly described|Fig.3.8|||||||||
29944|Greenbushes Pegmatite|43573|6|Mentioned|p325|||||||||
29944|Greenbushes Pegmatite|64580|6|Mentioned|map legend|||||||||
29944|Greenbushes Pegmatite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||2527+/-2 Ma||||Zoned pegmatite; tantalite-, spodumene-, and cassiterite-bearing.|
77864|Greenfields Gabbro|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2726 - 2650 Ma (inferred).||||Differentiated gabbro; cumulate to subophitic textures; hornblende-plagioclase-actinolite; metamorphosed.|
77864|Greenfields Gabbro|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2726-2650 Ma (inferred)||||Differentiated gabbro; cumulate to subophitic textures; hornblende--plagioclase--actinolite; metamorphosed|
77857|Greenmont Basalt|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2726 - 2699 Ma (inferred).|Coolgardie Subgroup|||Basaltic rock, vesicular, with rare pillows; metamorphosed; spinifex texture defined by metamorphosed actinolite.|
77857|Greenmont Basalt|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2726-2699 Ma (inferred)|Unit of Coolgardie Subgroup.|||Basaltic rock; vesicular, with rare pillows; metamorphosed; spinifex-like texture defined by metamorphic actinolite|
77857|Greenmont Basalt|73596|6|Mentioned|p1159, 1161-1162|||Coolgardie Inlier, Kalgoorlie Terrane.||||Overlies Burbanks Formation. Is overlain by Brilliant Formation.||
74808|Greensleeves Formation|64891|5|Briefly described|p37 Fig. 2,p39-40, p48-9 Tb. 1|Archean|Archean|Of Polelle Gp.Contains Woolgra Andesite Mbr.Conformable on Meekatharra Fm; conformable below Wilgie Mia Fm.+Wattagee Fm (Glen Gp) north of Cue. Age: 2760-2730Ma. Geological prov: Murchison Domain. Andesitic to rhyolitic volcanic-volcaniclastic rocks||||||07-FEB-11
74808|Greensleeves Formation|65546|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Polelle Group, Youanmi Terrane, Yilgarn Craton. Includes metasediments; meta felsic volcs, foliated, deeply weathered; felsic volcs and volcaniclastic rock, metamorphosed, deeply weathered and kaolinized; rhyolite, metamorphosed.||||||15-APR-11
74808|Greensleeves Formation|65548|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Polelle Group, Youanmi Terrane, Yilgarn Craton.  Schistose pelite, psammite with biotite porphyroblasts; banded iron-formation, ferruginous-banded chert; felsic volcs and volcaniclastic rock,  metamorphosed, deeply weathered and kaolinized||||||02-APR-13
74808|Greensleeves Formation|65550|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Polelle Group, Murchison Supergroup, Murchison Domain. Consists mainly of felsic volcanic and sedimentary rocks with minor basalt; all metamorphosed. Age dates from volcanic parts: c.2744 Ma, 2739 Ma||||||
74808|Greensleeves Formation|66195|5|Briefly described|p605|||In the Polelle Group. Felsic volcaniclastics and banded iron formations.||||||13-MAR-12
74808|Greensleeves Formation|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Mapped as eight separate but un-named units.||Unit in Polelle Group.|||Crystal-vitric rhyolite breccia and volcaniclastic sandstone; andesite; felsic volcanic and volcaniclastic rocks; dacitic schist; felsic schist; white to grey slate, highly fissile; schistose pelite and psammite.|
74808|Greensleeves Formation|67129|4|Described|p18 Fig.19, p20, p26-27, p30, p33-34|Archean|Archean|Murchison Domain, Youanmi Terrane. Widespread intermediate to felsic volcanism. REE plot.|c.2750 Ma.|Polelle Group|Includes Woolgra Andesite Member.|Is interbedded with Wilgie Mia Formation. Intruded by Yalgowra Suite.|Coarse-grained andesitic volcaniclastic rocks. Clasts are mainly intermediate to porphyritic dacitic in composition and fine-medium grained.|07-SEP-17
74808|Greensleeves Formation|68107|6|Mentioned|p618|||||Of the Polelle Group.|||Felsic volcanics and volcaniclastics.|
74808|Greensleeves Formation|68110|4|Described|p673, p674 Fig.2|Neoarchean|Neoarchean|Murchison Domain. |2761 +/- 4 Ma to 2734 +/- 4 Ma (U-Pb zircon).|Of the Polelle Group.|Includes Woolgra Andesite.|Conformably overlies Meekatharra Formation. Intruded by Glen Group sills. Is overlain conformably by Wilgie Mia Formation.|Andesitic to rhyolitic volcanic and volcaniclastic rocks.|
74808|Greensleeves Formation|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. U-Pb zircon age: 2747 +/- 5 Ma interpreted as the magmatic crystallization age of the dacite. From Geochron file 183338.1.pdf. Age of metarhyolite: 2746 +/- 4 Ma. From geochron file 185932.1.pdf.||Pollelle Group|Includes 13 unnamed subunits.|Conformably overlies Meekatharra Formation. Conformably overlain by Wilgie Mia Formation.|Andesitic to rhyolitic volcanic and volcaniclastic rocks; widely intruded by layered mafic-ultramafic sills; weakly metamorphosed|
74808|Greensleeves Formation|68698|5|Briefly described|p4-5, p7, p10-11, p18|Neoarchean|Neoarchean|Lu-Hf isotope data and source regions discussed.|c.2760-2740 Ma.|Polelle Group.|Woolgra Andesite Member.|Overlies Meekatharra Formation. Is overlain by Wilgie Mia Formation.|Andesitic to rhyolitic volcanic and volcaniclastic rocks.|
74808|Greensleeves Formation|69583|4|Described|p47, p49; Plate 2|Neoarchean|Neoarchean|Murchison Domain.|c.2760-2740 Ma.|Polelle Group.|Woolgra Andesite Member.|Is intruded by the Yalgowra Suite.|Andesitic to rhyolitic volcanic and volcaniclastic rocks; metamorphosed.|
74808|Greensleeves Formation|69584|5|Briefly described|p5 Fig.2, p54|Neoarchean|Neoarchean|Cue-Meekatharra area. ||Polelle Group|Woolgra Andesite|Overlies the Meekatharra Formation, overlain by the Wilgie Mia Formation.|Andesite and felsic volcaniclastic and volcanic rocks.|
74808|Greensleeves Formation|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Polelle Group.|Woolgra Andesite Member.|||
74808|Greensleeves Formation|69627|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Only appears in Interpreted Bedrock Geology legend.||Polelle Group|||Andesitic to rhyolitic volcanic and volcaniclastic rocks.|
74808|Greensleeves Formation|69628|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Shown in section only.|2760-2735 Ma|Polelle Group|||Andesitic to rhyolitic volcanic and volcaniclastic rocks; widely intruded by layered mafic-ultramafic sills; weakly metamorphosed (section only).|
74808|Greensleeves Formation|70020|4|Described|p117-118,123,129-130,132|Neoarchean|Neoarchean|Geological province: Yilgarn Craton. Thickness: <= 5 km. Intruded by widespread, thick and differentiated sills of Yalgowrie Suite. Contains felsic rocks associated with VHMS mineralization and are display prospective geochemical characteristics, simialr to Eelya Suite. Hosts Cu-Zn mineralisation.|2760-2740 Ma|Unit of Polelle Group.||Overlain by Wilgie Mia Formation. Underlain by Meekatharra Formation.|VHMS-bearing andesitic to rhyolitic volcanic and volcaniclastic rocks.|
74808|Greensleeves Formation|70030|4|Described|p189-190,192,205,207-208|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton. Thickness: 5km. Hosts the Hollandaire VMS deposit in the lower part of Greensleeves Formation, associated with Eelya and Cullculli suites felsic plutonism. Initial deposition of Greensleeves Formation likely coincides with felsic magmatism ca. 2760 Ma.|2760-2735 Ma|Unit of Polelle Group.|Includes Woolgara Andesite.|Overlain by Wilgie Mia Formation. Underlain conformably by Meekatherra Formation.|Well-bedded volcaniclastic rocks of andesitic composition that become more rhyolitic towards the top.|
74808|Greensleeves Formation|70139|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton. The four facies are mapped separately.||Polelle Group.|||Dacite and dacitic volcaniclastic rocks, weakly metamorphosed; felsic schist after volcanic rock, commonly deeply weathered; white to grey slate, highly fissile; undivided metamorphosed sedimentary rock.|
74808|Greensleeves Formation|70796|5|Briefly described|100k_geologyl_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv,  500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv,155568.1.pdf, 155569.1.pdf, 155572.1.pdf, 183338.1.pdf, 185922.1.pdf, 185927.1.pdf, 185932.1.pdf, 185957.1.pdf, 185959.1.pdf, 193972.1.pdf, 194757.1.pdf, Cue100_2443_stratig.pdf, Koonmarra100_2445_stratig.pdf, Madoonga100_2444_stratig.pdf, Nowthanna100_2643_stratig.pdf, Reedy100_2543_stratig.pdf, Tieraco100_2545_stratig.pdf. Numerous additional lithologies are discussed.|ca 2760 Ma2700 Ma (inferred)|Polelle Group|Includes the Woolgra Andesite Member.|Conformably overlain by the Wilgie Mia Formation. Conformably overlies the Meekatharra Formation. Intruded by the Yalgowra Suite.|Andesite; massive to fragmental, with siliceous clasts; pale grey weathering, silicified. Rhyolite to rhyolitic volcaniclastic rocks, massive to coarsely fragmental; metamorphosed sedimentary rock.|
74808|Greensleeves Formation|70830|4|Described|p5, p7, p9, p11, p14|Neoarchean|Neoarchean|Lithology at various localities is described.|c. 2760-2735 Ma|Polelle Group||Overlies the Meekatharra Formation. Overlain by the Wilgie Mia Formation. Intruded by the Yalgowra Suite.|Andesitic and rhyolitic volcanic and volcaniclastic rocks.|
74808|Greensleeves Formation|71148|6|Mentioned|p120|Neoarchean|Neoarchean|Cue Zone, northern Youanmi Terrane, Yilgarn Craton. Associated with VHMS mineralisation.|c.2760-c.2745 Ma.|||||
74808|Greensleeves Formation|71168|4|Described|p7-p8, p22|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Hosts VMS mineralization, and in petrochemically prospective areas copper-zinc occurences. See also p43, p52, p58, p60-p61.|c. 2760-2740 Ma|Polelle Group||Overlies the Meekatharra Formation. Overlain by the Wilgie Mia Formation. Intruded by the Yalgowra Suite.|Andesitic to rhyolitic volcanic and volcaniclastic rocks.|
74808|Greensleeves Formation|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). Wingate et al (2012) provided a zircon age of 2979+\-3 Ma as the magmatic age of a rhyolyte clast in volcaniclastic breccia. Sample GSWA 155569 (altered, recrystallised rhyolite) yielded a weighted mean 207Pb/206Pb date of 2977+\-3 Ma, interpreted to be the magmatic crystallisation age. Sample GSWA 183338 (metadacite) yielded a weighted mean 207Pb/206Pb date of 2747+\-5 Ma, interpreted to be the magmatic crystallisation age. Sample GSWA 185932 (metarhyolite) yielded a concordia age of 2746+\-4 Ma, interpreted to be the magmatic crystallisation age. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeol_lut.csv.|2760-2735 Ma|Unit of Poelle Group.|Includes Woolgra Andesite Member.|Overlain conformably by Wilgie Mia Formation. Underlain conformably by Meekatharra Formation. Intruded by Yalgowra Suite sills.|Volcanic and volcaniclastic rocks; felsic, rhyolitic, andesitic to rhyolitic, dacitic, widely intruded by layered mafic-ultramafic sills; weakly metamorphosed; schistose pelite and psammite; undivided sedimentary rocks interleaved with basalt.|
74808|Greensleeves Formation|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|2760-2735 Ma.|Polelle Group.|Woolgra Andesite Member.||Andesitic to rhyolitic volcanic and volcaniclastic rocks; widely intruded by layered mafic-ultramafic sills; weakly metamorphosed.|
74808|Greensleeves Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Youanmi Terrane.||Polelle Group|Includes Woolgra Andesite Member.||Andesitic to rhyolitic volcanic and volcaniclastic rocks; widely intruded by layered mafic--ultramafic sills; weakly metamorphosed.|
74808|Greensleeves Formation|72389|5|Briefly described|Map Legend|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Gabanintha 1:100k map sheet 2644.||Polelle Group|Includes the Woolgra Andesite Member.||Felsic volcaniclastic and volcanic rocks interleaved with sedimentary rocks; metamorphosed.|28-AUG-20
74808|Greensleeves Formation|72494|5|Briefly described|p15|||Youanmi Terrane, Yilgarn Craton.||Polelle Group.||Conformably overlies Meekatharra Formation. Is overlain conformably by the Wilgie Mia Formation.|Andesitic to rhyolitic volcanic and volcaniclastic rocks.|
74808|Greensleeves Formation|73596|6|Mentioned|p1170|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane.|2752 +/- 9 Ma.|Polelle Group.||||
31879|Greenvale Porphyry|22547|4|Described|p10|Orosirian|Orosirian|Age: 1865- 1850 Ma. Porphyric rock of Castlereagh Hill redefined as Greenvale Porphyry.||||||14-NOV-06
31879|Greenvale Porphyry|22754|5|Briefly described|p6|||||||||
31879|Greenvale Porphyry|23751|4|Described|p8|Proterozoic|Proterozoic|Of Paperbark Supersuite.||||||
31879|Greenvale Porphyry|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1850Ma. Geological province: Kimberley Province (East).||||||07-FEB-11
31879|Greenvale Porphyry|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
31879|Greenvale Porphyry|43853|5|Briefly described|Map Legend||Proterozoic|||||||
31879|Greenvale Porphyry|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|In the Lamboo Complex.||||||14-NOV-06
31879|Greenvale Porphyry|44230|5|Briefly described|Map Legend||Proterozoic|||||||
31879|Greenvale Porphyry|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31879|Greenvale Porphyry|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Paperbark Supersuite.||||||07-NOV-08
31879|Greenvale Porphyry|63866|5|Briefly described|p132|||Co-magmatic with the Whitewater Volcanics and the Castlereagh Hill Porphyry.||||||
31879|Greenvale Porphyry|64731|5|Briefly described|p164|Paleoproterozoic|Paleoproterozoic|In Hooper Complex and Western Zone of Hall Creek Orogen.|1860 - 1850 Ma.|||||12-APR-12
31879|Greenvale Porphyry|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Paperbark Supersuite|||Dark grey, porphyritic micromonzogranite; medium- to coarse-grained phenocrysts of quartz, K-feldspar, and plagioclase.|31-JUL-15
31879|Greenvale Porphyry|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Paperbark Supersuite|||Dark grey, porphyritic micromonzogranite; medium to coarse grained phenocrysts of quartz, K-feldspar and plagioclase.|
31879|Greenvale Porphyry|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone.|1855-1855 Ma (Isotopic)|Unit of Paperbark Supersuite.|||Dark grey, porphyritic micromonzogranite; medium- to coarse-grained phenocrysts of quartz, K-feldspar, and plagioclase|
31879|Greenvale Porphyry|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1855 Ma|Paperbark Supersuite|||Dark grey, porphyritic micromonzogranite, medium-coarse grained phenocrysts of quartz, k-feldspar and plagioclase.|
31879|Greenvale Porphyry|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1855+\-4 Ma (isotopic)|Unit of Paperbark Supersuite.|||Dark grey, porphyritic micromonzogranite; medium- to coarse-grained phenocrysts of quartz, K-feldspar, and plagioclase|
31879|Greenvale Porphyry|72437|5|Briefly described|p5, p38-39|||Lamboo Complex. Co-magmatic with the Whitewater Volcanics.|||||Feldspar-quartz porphyry.|
73504|Gregory Range Suite|63417|5|Briefly described|Map legend|Archean|Archean|Geological Province: Fortescue Basin. Metamorphosed granitic rocks; foliated and gneissic. Granophyre; locally includes gneissic granophyre and granophyric gneiss.||||||07-NOV-08
73504|Gregory Range Suite|64580|4|Described|map legend||Neoarchean|Undivided granitoid rock ; well foliated.||||||15-DEC-08
73504|Gregory Range Suite|66217|6|Mentioned|p46.|||Coeval with Koongaling Volcanic Member of Hardey Formation.||||Intrudes Hardey Formation.||
73504|Gregory Range Suite|67202|4|Described|p49, p51, p54, p64, p224, p232, p281|Archean|Archean|Pilbara Craton. Crops out as a narrow, N-trending, 5-10km wide linear belt over 150km in length. Thought to be coeval and comagmatic with felsic rocks in the Hardey Formation. Poorly- to moderately-magnetised. Locally rich in U. Appears as Gregory Suite on p232.|c.2760 Ma (Nelson, 1996).|||Faulted against and underlies Hardey Formation. Underlies Tarcunyah Group.|Granites: syenogranite, granitic gneiss and granophyre.|
73504|Gregory Range Suite|68902|6|Mentioned|p5 fig 3|Neoproterozoic|Neoproterozoic|||||||
73504|Gregory Range Suite|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean||||||Metamorphosed medium -to coarse-grained syenogranite; sheared, foliated, and gneissic. Fine grained to microporphyritic granitic rock; granophyre locally including gneissic granophyre and granophyric gneiss.|
73504|Gregory Range Suite|69590|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Events: Fortescue Rifting Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|3763-3757 Ma (inferred)||||Medium -to coarse-grained porphyritic to seriate (meta)syenogranite; sheared, foliated, and gneissic; granophyre, gneissic granophyre, granophyric gneiss.|
73504|Gregory Range Suite|70826|6|Mentioned|p8|Neoarchean|Neoarchean|Intrudes the eastern Pilbara Craton.|||||Granites.|
73504|Gregory Range Suite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite, augen gneiss, granophyre|
73504|Gregory Range Suite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Fortescue Basin. Unnamed granophyric sub-unit distinguished.|Max age 2763+/-8 Ma. Min 2757+/-5 Ma.||||Metamorphosed granitic rocks; moderate to strong tectonic foliation. Granophyre; locally includes gneissic granophyre, and granophyric gneiss.|
75309|Gregory Range Suite - granophyre 75309|63417|5|Briefly described|Map legend|Archaean|Archaean|Geological Province: Fortescue Basin.Granophyre; locally includes gneissic granophyre and granophyric gneiss.||||||
33917|Gregory Well gneiss|22449|6|Mentioned|Table3 P27||Archean|Age of unit is 3115 Ma||||||07-NOV-08
78696|Grey Member|69788|3|Fully described|p1023, p1029-1030, p1035, p1037|Pleistocene|Pleistocene|New name, after the settlement of Grey. Type locality and outcrop mentioned. Partly retains original aragonite and high-Mg calcite mineralogy of the bioclasts. The eolianite was covered by a layer of massive calcrete and later a paleosol.|74 +/- 9 ka (U/Th), Lipar and Webb, 2014.|Unit in Tamala Limestone.||Coeval with Minim Cove Member.|Consists of an eolian calcarenite/calcrete-microbialite/paleosol cycle.|
78696|Grey Member|69840|4|Described|p185, p187, p187 Tb.1, p190, p198, p200|Pleistocene|Pleistocene|Dating using U/Th geochronology. Marine Isotope stage 4-5.|0.07400 +/- 0.00900 Ma|Tamala Limestone|||Microbialite. c. 22% aragonite remaining calcite.|
40137|Grimwade Suite|61246|6|Mentioned|p3, p22|||Includes The Granites Granite?||||||21-SEP-06
40137|Grimwade Suite|61405|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Medium- to coarse-grained, sometimes porphyritic, tourmaline-muscovite-bearing biotite granite; medium-grained granodiorite; strongly foliated to foliated. Geological Province: Arunta region - Aileron Province.||||||07-NOV-08
40137|Grimwade Suite|62628|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Tanami Inlier. Coarse and fine grained, porphyritic and non porphyritic biotite or hornblende bearing syenogranite to monzogranite.||||||07-NOV-08
40137|Grimwade Suite|62632|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Tanami/Arunta Region-Aileron Province. Granite, monzogranite, gneiss.||||||07-NOV-08
40137|Grimwade Suite|62637|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region. Various unnamed granites, granodiorites.||||||07-NOV-08
40137|Grimwade Suite|63261|4|Described|p9 Fig. 5, p16|Paleoproterozoic|Paleoproterozoic|The Coomarie Supersuite of Dean (2001). Includes Slatey Creek, The Granites and Lewis Granites of Blake et al (1979), and parts of Browns Range and Frankenia granite complexes. Interpreted crystal'n ages between: 1821+/-4 and 1791+/-4Ma (Smith 2001).||||||26-NOV-15
40137|Grimwade Suite|64662|5|Briefly described|p30 Fig. 3|Statherian|Orosirian|Age: 1825-1790Ma. Geological Province: Tanami region. Also referred to as Grimwade suite granites - see p44.||||||07-FEB-11
40137|Grimwade Suite|64725|5|Briefly described|p63 Fig.7.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|1820-1790 Ma.|||||
40137|Grimwade Suite|64733|5|Briefly described|p170 Fig.2, p172 Fig.4, p175|Statherian|Orosirian|Low aeromagnetic response.|1820-1790 Ma.|||||20-APR-12
40137|Grimwade Suite|64734|5|Briefly described|p186 Fig.1|Statherian|Orosirian|1820-1790 Ma||||||14-SEP-09
40137|Grimwade Suite|65358|5|Briefly described|p6-7|Statherian|Orosirian|In Tanami Region. Dominated by metaluminous I-type biotite granodiorite and monzogranite. Intruded between 1825-1790 Ma.||||||
40137|Grimwade Suite|65359|5|Briefly described|p23, p26-28 Figs.26-28.|||Tanami Region. Felsic plutons with weak to no magnetic signature.||||||
40137|Grimwade Suite|66129|6|Mentioned|p213, p214 Fig.1|Statherian|Orosirian|1820-1790 Ma.||||||
40137|Grimwade Suite|67163|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.|||||Granite, monzogranite; fine-, medium- and coarse-grained, K-feldspar megacrysts, metasedimentary xenoliths.|20-OCT-11
40137|Grimwade Suite|67165|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province. Parts of this unit are mapped according to their lithologies and the strength of their magnetic responses.|||||Granites, granodiorites and granite gneiss.|
40137|Grimwade Suite|67824|6|Mentioned|p385 Fig.2|Statherian|Orosirian||~1820-1790 Ma|||||
40137|Grimwade Suite|67826|6|Mentioned|p401 Fig.2|Statherian|Orosirian||1820 - 1790 Ma|||||
40137|Grimwade Suite|68474|6|Mentioned|p572|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen.|1820-1790 Ma|||||
40137|Grimwade Suite|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleoproterozoic|Paleoproterozoic|See also 100k_maginterpgeop_lut.csv. Granites-Tanami Complex.|c.1820-1790 Ma (Huston et al., in press).||||Granite.|
40137|Grimwade Suite|69003|5|Briefly described|p5, p17 Fig.21|||Granites-Tanami Orogen.|1820-1790 Ma.|||||
40137|Grimwade Suite|69253|5|Briefly described|p747 Fig.1, p755-760, p763, p765 Fig.21|Statherian|Orosirian|Petrophysical properties detailed. See also p766.|c.1825-1790 Ma.|||||
40137|Grimwade Suite|69417|5|Briefly described|p2:5|Orosirian|Orosirian|Tanami Region.||||Intrudes Ware Group.||12-JUL-16
40137|Grimwade Suite|69426|4|Described|p11:4 Fig.11.3, 11:10-12, 14, 21, 24, 26|Statherian|Orosirian|Widely distributed. Also includes parts of the Browns Range, Frankenia and Coomarie Domes, and granites in the Apertowonga Range - MacFarlanes Peak and Officer Hill - Muriel Range areas. Weakly to non-magnetic. Geochemistry briefly described. Gold mineralisation at The Granites goldfield is coincident with the margin of a pluton of this Suite. One pluton intruding the Quorn Au deposit in The Granites goldfield is dated at 1815 +/- 4 Ma (Smith, 2001).|1821-1791 Ma.||Slatey Creek, The Granites, Lewis, Coomarie, Browns Range and Frankenia Granites.|Intrudes Mount Charles Formation.|Monzogranite, syenogranite.|12-JUL-16
40137|Grimwade Suite|69427|5|Briefly described|p12:3, 20, 22|Statherian|Orosirian|Vandenberg et al. (in prep.). Aileron Province. Poor, scattered outcrops extending NW into the Tanami Region. Derived from partial melting of late Archean gneiss, with minor assimilation of Paleoproterozoic sedimentary rocks.|c.1805-c.1785 Ma.||||Granites, most commonly porphyritic, with compositions ranging from monzogranite to syenogranite; coarse- to fine-grained, porphyritic to non-porphyritic.|12-JUL-16
40137|Grimwade Suite|69432|6|Mentioned|p17:2|||||||Is overlain unconformably by the Birrindudu Group.||12-JUL-16
40137|Grimwade Suite|69440|5|Briefly described|p25:2|||||||Is overlain unconformably by Munyu Sandstone.|Granites.|12-JUL-16
40137|Grimwade Suite|69618|6|Mentioned|p90|Paleoproterozoic|Paleoproterozoic||c.1825-1790 Ma.|||||
40137|Grimwade Suite|69673|6|Mentioned|p3|||||||||
40137|Grimwade Suite|69747|5|Briefly described|p263-p264|Orosirian|Orosirian|Geological province: Tanami Block, North Australian Craton. Associated with late syn- to postcollisional tectonic settings within a ~30 Ma million year long period of magmatic activity broadly spanning ca. 1825-1791 Ma (Smith, 2001). Granitic plutons derived from a crustal source in response to continental thickening after collision between the Granites-Tanami Orogen and the Arunta Orogen around 1795 Ma.|ca. 1825-1790 Ma|||||25-JUN-19
40137|Grimwade Suite|70291|4|Described|p178,180-181,191|Sthatherian|Orosirian|Geological province: Tanami. Occurred after deposition of Mount Charles Formation (post D3 event).|1820-1790 Ma||||Non-magnetic, peraluminous biotite monzogranite to syenogranite with hornblende in SiO2-poorer samples.|
40137|Grimwade Suite|70478|4|Described|p2 Fig 1, 8-9, 11-13, p39 App 3|Orosirian|Orosirian|Geological Province: Tanami. Granites drilled in drillholes TAN99DDH7, TAN99DDH15, TAN99DDH21, TAN99DDH23, TAN99DDH28 assigned to Grimwade Suite. See associated drilling summaries and appendices for more detail. SHRIMP U-Pb magmatic zircon ages of 1805+\-6 Ma (DDH7 monzogranite; Smith 2001); 1812+\-5 Ma (DDH15 monzogranite; Claoue-Long et al., 2001); 1809+\-3 Ma (DDH21 granodiorite; Cross et al., 2005); 1808+\-3 Ma (DDH23 monzogranite; Cross et al., 2005); 1844+\-4 Ma (DDH28 monzogranite; Claoue-Long et al., 2001).||||Intrudes Mount Charles Formation, Dead Bullock Formation.|monzogranite, syenogranite|11-OCT-19
40137|Grimwade Suite|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.|1821-1791 Ma.||||Coarse- and fine-grained, porphyritic and non-porphyritic biotite- or hornblende-bearing monzogranite, syenogranite.|
40137|Grimwade Suite|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.|1821-1791 Ma.||||Biotite +/- hornblende syenogranite to monzogranite: coarse- and fine-grained, equigranular to porphyritic.|
40137|Grimwade Suite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, granite|
40137|Grimwade Suite|71348|6|Mentioned|p201|Orosirian|Orosirian|Geological province: Aileron Province, Arunta Region.||||||
40137|Grimwade Suite|71349|5|Briefly described|p724-725|Paleoproterozoic|Paleoproterozoic|Tanami Region.|1825-1790 Ma.|||Intrudes Tanami and Ware Groups.||
40137|Grimwade Suite|73089|5|Briefly described|p3, p8, p39|Statherian|Orosirian|Granites-Tanami Orogen and northwestern Aileron Province. Broadly coeval with other granites of the orogen but distinguished by differences in magnetic character (Ahmad et al., 2013). A date of 1785 +/- 4 Ma for a granite in the Aileron Province might represent a younger component.|1821-1791 Ma||Lewis Granite|||
40137|Grimwade Suite|73158|5|Briefly described|p2|Statherian|Orosirian|Granites-Tanami Orogen.|1821-1791 Ma||||Granitic intrusions.|
40137|Grimwade Suite|73159|5|Briefly described|p2|||Granites-Tanami Orogen.|1821-1791 Ma.||||Granites.|
25034|Gumhole Formation|22741|5|Briefly described|P24||Late Devonian|||||||
25034|Gumhole Formation|22767|5|Briefly described|Table3 P18, P20||Late Devonian|||||||
25034|Gumhole Formation|22776|4|Described|Table.3|Late Devonian|Late Devonian|Parent: Fairfield Group||||||
25034|Gumhole Formation|23722|5|Briefly described|p34|Early Carboniferous|Late Devonian|Parent: Fairfield Group.  Geological Province: Canning Basin.||||||24-NOV-08
25034|Gumhole Formation|23766|5|Briefly described|p15|Early Carboniferous|Late Devonian|Parent: Fairfield Group.||||||24-NOV-08
25034|Gumhole Formation|24370|5|Briefly described|p39|||Geological Province: Canning Basin.||||||
25034|Gumhole Formation|36224|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Of the Fairfield Group.  Limestone, siltstone, shale, sandstone; minor dolomite.  Late Devonian to Early Carboniferous.||||||01-FEB-05
25034|Gumhole Formation|36225|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
25034|Gumhole Formation|36634|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
25034|Gumhole Formation|38277|6|Mentioned|p154|||||||||
25034|Gumhole Formation|40838|6|Mentioned|p280|||||||||
25034|Gumhole Formation|40866|6|Mentioned|p181|||||||||
25034|Gumhole Formation|41023|4|Described|p288|||||||||
25034|Gumhole Formation|41111|6|Mentioned|Fig.4|||||||||
25034|Gumhole Formation|41113|6|Mentioned|p515|||||||||
25034|Gumhole Formation|41158|6|Mentioned|p80|||||||||
25034|Gumhole Formation|41217|6|Mentioned|p310|||||||||
25034|Gumhole Formation|41730|6|Mentioned|Fig.3|||||||||
25034|Gumhole Formation|41839|4|Described|p21|||||||||
25034|Gumhole Formation|42030|5|Briefly described|p746|||||||||
25034|Gumhole Formation|42032|6|Mentioned|p513|||||||||
25034|Gumhole Formation|42347|6|Mentioned|Fig.2 P1020|||||||||
25034|Gumhole Formation|42547|5|Briefly described|p92|||||||||
25034|Gumhole Formation|42811|5|Briefly described|p43|||of Fairfield Group||||||
25034|Gumhole Formation|42814|6|Mentioned|p23|||||||||
25034|Gumhole Formation|42860|5|Briefly described|Fig.2|||||||||
25034|Gumhole Formation|42880|5|Briefly described|Fig.2,p1020|||||||||
25034|Gumhole Formation|42933|5|Briefly described|Fig.94 p258|||||||||
25034|Gumhole Formation|43173|6|Mentioned|54||Early Permian|||||||
25034|Gumhole Formation|43563|6|Mentioned|Fig.5,p10||Late Devonian|||||||
25034|Gumhole Formation|43723|6|Mentioned|p51||Devonian|||||||
25034|Gumhole Formation|43818|6|Mentioned|Table 2,p42|||||||||
25034|Gumhole Formation|44143|4|Described|p.437 Table 4-19|Carboniferous|Devonian|Unit in Fairfield Group. Up to 370m thick; limestone interbedded with siltstone, shale and claystone; shallow marine. Conformably overlies Luluigui Formation. Type section along Great Northern Highway (NOONKANBAH: 18 deg 07' 30" S, 125 deg 27' 25" E). Varied invertebrate fauna.||||||
25034|Gumhole Formation|45133|4|Described|p2|||||||||
25034|Gumhole Formation|45143|2|Defined|p8|Famennian|Famennian|||||||
25034|Gumhole Formation|45153|2|Defined|App.3-40|late Famennian|late Famennian|||||||
25034|Gumhole Formation|45158|4|Described|p22|||||||||
25034|Gumhole Formation|46794|5|Briefly described|p64|||||||||
25034|Gumhole Formation|48978|4|Described|p4|||Geochemistry P9 etc.||||||
25034|Gumhole Formation|64187|5|Briefly described|p320 Fig. 2|Famennian|Famennian|Formation is Fm. In text. Underlain by Nullara Limestone, overlain by Yellow Drum Formation. Limestone, siltstone, dolomite, shale, sandstone (shallow marine). Geological Province: Canning Basin.||||||08-FEB-10
25034|Gumhole Formation|64580|6|Mentioned|map legend|||Of Fairfield Group.||||||15-DEC-08
25034|Gumhole Formation|64643|5|Briefly described|p3 Fig. 2|Missippippian|Missippippian|||||||
25034|Gumhole Formation|64981|5|Briefly described|p669 Fig.3, p670.|Famennian|Famennian|||Unit in Fairfield Group.||Is overlain by Yellow Drum Formation.|Shallow marine muds and carbonates.|
25034|Gumhole Formation|65214|6|Mentioned|p280|Devonian|Devonian|Canning Basin. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
25034|Gumhole Formation|65301|5|Briefly described|p5 Fig. 4|Mississippian|Mississippian|Of Fairfield Group. Geological province: Canning Basin.||||||
25034|Gumhole Formation|65449|6|Mentioned|p6|Early Carboniferous|Early Carboniferous|||Fairfield Group.||||
25034|Gumhole Formation|66127|5|Briefly described|p442-443, Plates 2, 7.|Famennian|Famennian|||Basal unit in Fairfield Group.||Unconformably overlies Windjana and Nullara Limestones. Is overlain  by Yellow Drum Sandstone.|Shallow-marine limestone, siltstone and shale; minor dolomite.|
25034|Gumhole Formation|66498|6|Mentioned|p46|Carboniferous|Carboniferous|Canning Basin. Contains a rich and diverse micro- and macro-vertebrate fossil assemblage (described).||||||
25034|Gumhole Formation|67131|6|Mentioned|p2, p3 Fig. 2, p5-7|Tournaisian|Famennian|Fig. 2 says this unit "includes the 'May River Shale' in the subsurface" [?].||Fairfield Group||||
25034|Gumhole Formation|68007|6|Mentioned|p4|Late Devonian|Late Devonian|Canning Basin.||||||25-FEB-20
25034|Gumhole Formation|68297|5|Briefly described|p195|Famennian|Famennian|Includes Expansa zone microvertebrate assemblages, but ranges to the top of the Devonian.||||||
25034|Gumhole Formation|68902|5|Briefly described|p9 fig 5|Devonian|Devonian|Overlies (mainly Upper) Devonian reef complexes.||Fairfield Group.||Overlain by Yellow Drum Formation.||
25034|Gumhole Formation|69099|5|Briefly described|500k_geologyp08_lut.csv|Tournasian|Famennian|||Fairfield Group||||
25034|Gumhole Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Tournaisian|Famennian|||||||
25034|Gumhole Formation|69182|6|Mentioned|Ch4 p9, Ch4 p13-p14|Famennian|Famennian|North Canning Basin. See also Ch4 p45, Ch4 p47, Ch4 p50-p58, Ch4 p74, Ch4 p84, Ch4 p86.||Fairfield Group||Overlain by the Yellow Drum Formation.||
25034|Gumhole Formation|69297|6|Mentioned|p337, p352|Tournaisian|Tournaisian|Broome Platform of the Canning Basin. ||Fairfield Group||Overlies the Luluigui Formation. Overlain by the Yellow Drum Sandstone.||
25034|Gumhole Formation|69312|5|Briefly described|p3, p19, p23 fig 27|Tournaisian|Famennian|Canning Basin. Shown as Gum Hole p19.||Fairfield Group||Overlies the Luluigui Formation and the Nullara Sequence. Overlain by the Yellow Drum Formation.|Carbonate shales, marl.|11-FEB-20
25034|Gumhole Formation|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Fairfield Group.||||
25034|Gumhole Formation|70272|5|Briefly described|p882|Tournaisian|Famennian|Lennard shelf, Canning Basin. Has the highest concentration of Pb and Zn of units in this Group.||Fairfield Group.||||
25034|Gumhole Formation|70492|5|Briefly described|p166, 175, 178, 180-181|Late Devonian|Late Devonian|Canning Basin. Sequence (stratigraphy) development diagram.||Fairfield Group.||Is overlain by Yellow Drum Formation.|Limestone with minor dolostone, siltstone and sandstone. Bioclastic shoals dominated by bryozoans.|
25034|Gumhole Formation|70774|5|Briefly described|p4|Late Devonian|Late Devonian|Fitzroy Trough and Lennard Shelf, Canning Basin.||Fairfield Group||Overlain by the Yellow Drum Formation.||10-FEB-20
25034|Gumhole Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Fairfield Group.|||Shallow marine colour laminated and cross bedded fossiliferous limestone interbedded with siltstone and shale, and minor sandstone and dolomite|
25034|Gumhole Formation|71892|6|Mentioned|p10|Paleozoic|Paleozoic|||||||
25034|Gumhole Formation|71894|5|Briefly described|p4|Famennian|Famennian|Canning Basin.||||Overlain by the Yellow Drum Formation.|Carbonate and shale.|
25034|Gumhole Formation|72499|5|Briefly described|p7 Fig.6.|Fammennian|Fammennian|Located in the Fitzroy Trough.||?Fairfield Group.||Underlies Yellow Drum Formation.|Includes carbonate shales.|
25034|Gumhole Formation|72502|4|Described|p1, p3, p5-6, p16-18, p21, p23|upper Famennian|upper Famennian|Lennard Shelf, Canning Basin. Best exposed at Oscar Hill. Yielded a chondrichthyan fauna including[?] Thrinacodus ferox, Cladodus thomasi, Protacrodus aequalis and Deihim mansureae. [Article includes detailed systematic palaeontology]. Includes shoal facies. Probably underlain by Nullara Limestone at Horseshoe Range and Red Bluffs, and possibly by Luluigui Formation at Napier and Oscar Ranges. The low numbers of recovered teeth prevented the application of the biofacies model [of Ginter, 2000].||Fairfield Group||Probably underlain by Nullara Limestone. Possibly underlain by Luluigui Formation. Overlain by Yellow Drum Formation.|Consists mostly of bioclastic and oolitic sandy limestone with interbedded carbonate, siltstone and shale.|
25034|Gumhole Formation|73117|5|Briefly described|p3|Famennian|Famennian|Canning Basin.||Fairfield Group||Disconformably underlain by Reef Complex. Overlain[?] by Yellow Drum Formation.|Dominantly carbonate-shale, marl.|
25039|Gussys zoned pegmatite|34723|5|Briefly described|p239|||||||||
75621|Gwynne Creek Gneiss|68186|4|Described|p3 Fig.2, p8, p11, p26-27, p31, p36-37|Mesoproterozoic|Mesoproterozoic|See also p54, p60, p82, p85-88, Plates 1A, 2. Arid Basin, Albany-Fraser Orogen. Substantially sourced from Biranup Zone. A single analysis gave a maximum age of 1483 +/- 12 Ma. Metamorphosed at c.1297 Ma, c.1270 Ma and c.1193 Ma. Geochronology and deformation detailed. Initial-Hf evolution plots.|1533 +/- 11 Ma (maximum depositional age).||||Mainly psammitic and semipelitic gneisses; also layered, finely laminated, quartzofeldspathic gneiss with layer-parallel leucosomes, minor metagranitic, metamafic and meta-ultramafic rocks; intruded by late coarse-grained K-feldspar-rich pegmatites.|
75621|Gwynne Creek Gneiss|68654|5|Briefly described|p2 fig 1, p3|Mesoproterozoic|Mesoproterozoic|Arid Basin, Albany-Fraser Orogen.|? - 1330 Ma?||||Metasedimentary rocks.|
75621|Gwynne Creek Gneiss|69003|6|Mentioned|p28, p43|||Arid Basin, Albany-Fraser Orogen. Records uplift and associated brittle deformation during the period c.1260-1225 Ma.||||||
75621|Gwynne Creek Gneiss|69140|6|Mentioned|p1|||Geological province: Albany-Fraser Orogen. ||||||
75621|Gwynne Creek Gneiss|69252|5|Briefly described|p7 Fig.3, p16, p19|||Arid Basin. Located between the Biranup and Fraser Zones, NE Albany-Fraser Orogen. Underwent high-T metamorphism between 1270 and 1193 Ma.|1483 +/- 12 Ma (maximum deposition age).||||Mainly psammitic gneiss interlayered with thin layers of semipelitic gneiss. Also layers of finely laminated quartzofeldspathic gneiss, and minor metagranite, metamafic and meta-ultramafic rocks.|
75621|Gwynne Creek Gneiss|69386|5|Briefly described|p4, p6|Mesoproterozoic|Mesoproterozoic|Fraser and Nornalup Zones, Albany-Fraser Orogen.|||||Psammitic gneiss.|
75621|Gwynne Creek Gneiss|69595|5|Briefly described|p3 fig 1, p19, p20, p21 fig 8, |Calymmian|Calymmian|Eastern Biranup or Eastern Nornalup Zones, Arid Basin. Exposed over 200km. Metamorphism occurred at 1270 +/- 11 Ma. Hf ages range from 1626 +/- 10 Ma to 1650 Ma. See also p22, p23 tbl 4, p24 tbl 5, p24, p33, p34 fig 20, p40, p44, p57.|1533 +/- 11 - 1483 +/- 12 Ma (U-Pb zircon).||||Psammitic and semipelitic gneiss and also includes layered, finely laminated, quartzofeldspathic gneiss with layer-parallel leucosomes.  Minor metagranitic, metamafic and meta-ultramafic rocks intrude the metasedimentary rocks.|
75621|Gwynne Creek Gneiss|69743|6|Mentioned|p190-191|Mesoproterozoic|Mesoproterozoic||1480-1345 Ma.|||||
75621|Gwynne Creek Gneiss|70023|6|Mentioned|p167|||Geological province: Albany-Fraser Orogen. Also of Arid Basin.||||||
75621|Gwynne Creek Gneiss|70084|6|Mentioned|p219|||Geological province: Albany-Fraser Orogen, Yilgarn Craton.||||||
75621|Gwynne Creek Gneiss|70089|6|Mentioned|p262-263|Mesoproterozoic|Mesoproterozoic|Arid Basin, NE Albany-Fraser Orogen.|||||Psammitic gneiss with minor semipelitic layers.|
75621|Gwynne Creek Gneiss|70090|4|Described|p442-444,447,449-450,452-454,460,462|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen, West Australian Craton. Of Arid Basin. Maximum depositional age: c. 1533 Ma. Minimum depositional age: constrained by 1270+\-11 Ma metamorphism. Paleoproterozoic detrital zircon age components include c. 1739, 1677, 1657, 1607 1533, and 1528 Ma. Mesoproterozoic age components include c. 1484 Ma. Contains most dominant population of 1700-1650 Ma detrital zircon age components in the Arid Basin and minor 1825-1725 Ma components. Zircons are metamict, however Lu-Hf isotopic analysis reveals the primary source being Biranup Zone material, or remelted equivalents.||||||
75621|Gwynne Creek Gneiss|70182|6|Mentioned|p2-3, p5, p9-10, p15, p34|||Arid Basin, NE Albany-Fraser Orogen. Affected by Stage I (1330-1260 Ma) tectonism.||||||
75621|Gwynne Creek Gneiss|70254|6|Mentioned|p357|||Geological province: Albany-Fraser Orogen.||||||
75621|Gwynne Creek Gneiss|70256|5|Briefly described|p3, p5|Mesoproterozoic|Mesoproterozoic|Arid Basin, Albany-Fraser Orogen.|||||Psammitic gneiss with minor semipelitic layers.|
75621|Gwynne Creek Gneiss|70732|6|Mentioned|p285,299|||Geological province: Albany-Fraser Orogen. Of Arid Basin.||||||
75621|Gwynne Creek Gneiss|70735|6|Mentioned|p28|||Arid Basin, Fraser Zone, Albany-Fraser Orogen.||||||
75621|Gwynne Creek Gneiss|70802|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen, West Australian Craton. Of Arid Basin. Events: Albany-Fraser Orogeny Stage II (1225-1140 Ma); Albany-Fraser Orogeny (1330-1140 Ma); Albany-Fraser Orogeny Stage I (1330-1260 Ma). Sample GSWA 182431 (psammitic gneiss) yielded a concordia age of 1466+\-4 Ma, interpreted as maximum depositional age of sandstone protolith; and metamorphism at 1298+\-7 Ma. Sample GSWA 182432 (semipelitic gneiss) yielded a weighted mean 207Pb*/206Pb* date of 1533+\-18 Ma, interpreted as maximum depositional age of the sandstone protolith. Sample GSWA 194735 (quartzofeldspathic gneiss) yielded concordia ages of 1657+\-5 Ma and 1270+\-11 Ma, interpreted age of pervasive migmatisation, and metamorphic zircon rim growth respectively. See 500k_interpgeop14_lut.csv, 250k_pre_mesozoic_interpgeop_lut.csv.|1483+\-12 Ma; 1297+\-7 Ma||||Psammitic gneiss with minor semipelitic layers; includes minor metagranitic rocks, metamafic, and meta-ultramafic rocks|
75621|Gwynne Creek Gneiss|70813|6|Mentioned|p3|||Arid basin.||||||
75621|Gwynne Creek Gneiss|70826|6|Mentioned|p10|Mesoproterozoic|Mesoproterozoic|Albany-Fraser Orogen. Misspelt Gwynn Creek Gneiss.||||||20-MAY-20
75621|Gwynne Creek Gneiss|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Arid Basin.|Max age 1483+/-12 Ma, Min 1297+/-7 Ma.||||Psammitic gneiss with minor semipelitic layers; includes minor metagranitic rocks, metamafic, and meta-ultramafic rocks.|
75621|Gwynne Creek Gneiss|72059|6|Mentioned|p57|Mesoproterozoic|Mesoproterozoic|Geological province: Fraser Zone, Albany-Fraser Orogen. Of Arid Basin.||||||
75621|Gwynne Creek Gneiss|72710|6|Mentioned|p4 Fig.2.|Mesoproterozoic|Mesoproterozoic|Part of Arid Basin, Albany-Fraser Orogen.|1600 Ma to 1310 Ma.||||Includes gneiss.|
75621|Gwynne Creek Gneiss|73084|6|Mentioned|p12|||Albany-Fraser Orogen, Kepa Kurl Booya Province, Biranup Zone and Fraser Zone.||||||
75621|Gwynne Creek Gneiss|73597|6|Mentioned|p1178|||Albany-Fraser Orogen.||||||
79160|Haig Cave Supersuite|70090|6|Mentioned|p455|||||||||
79160|Haig Cave Supersuite|70182|5|Briefly described|p7|Mesoproterozoic|Mesoproterozoic|Madura Province, Albany-Fraser Orogeny.|1410-1400 Ma.||||Weakly layered, medium-grained, mafic cumulate rocks, locally with peridotitic cumulate rocks, intruded by medium- to coarse-grained plagiogranite.|
79160|Haig Cave Supersuite|70802|4|Described|250k_pre_mesozoic_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Madura Province. Events: Maralinga Event (1200-1100 Ma); Madura Province events (1900-1330 Ma). Sample GSWA 206754 (metagranodiorite) yield a weighted mean 207Pb*/206Pb* date of 1389+\-7 Ma, interpreted as the magmatic crystallization age of the granodiorite. See also geochron files.|1415+\-7 Ma; 1389+\-7 Ma||||Metagabbro interlayered with trondhjemitic plagiogranite; locally includes peridotitic cumulate; may inlude intrusions of Moodini Supersuite|
79160|Haig Cave Supersuite|70813|6|Mentioned|p22|Mesoproterozoic|Mesoproterozoic||c. 1400 Ma|||||
79160|Haig Cave Supersuite|70831|5|Briefly described|p25-p26|Ectasian|Calymmian|Madura Province.|c. 1415-1389 Ma|||||
79160|Haig Cave Supersuite|71143|5|Briefly described|p427,429-431,433-434,437,440|Calymmian|Calymmian|Geological province: Madura Province. Contains with mantle-like isotope values interpreted as melting of subduction-modified N-MORB source. Interlayered granitic and gabbroic rocks yielded U-Pb zircon dates of 1415-1389Ma, interpreted as magmatic crystallization ages (Nelson, 2005a, 2005b, 2005c; Kirkland et al., 2013b, 2013c; Wingate et al., 2016b). Intruded by medium- to coarse-grained trondhjemitic plagiogranite of the Loongana Arc (oceanic-arc complex; Spaggiari et al., 2015b). Geochemical analysis indication N-MORB affinities with contribution from subduction related mafic magmas (see p430). No known rocks equivalent in age to the Haig Cave Supersuite in the Coompana Province.|1415-1389 Ma||||Tholeiitic mafic/ultramafic intrusive rocks.|
79160|Haig Cave Supersuite|71165|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Madura Province.|c.1400 Ma.||||Metagabbro interlayered with trondhjemitic plagiogranite.|
79160|Haig Cave Supersuite|71488|6|Mentioned|p153|||||||||
79160|Haig Cave Supersuite|71618|5|Briefly described|p129,133,135|Mesoproterozoic|Calymmian|Geological province: Madura Province. Possible source for c. 1412 Ma zircon peak in the Shanes Dam Conglomerate.|1409+\-6 Ma (mean age; Wingate et al., 2015)|||||06-SEP-19
79160|Haig Cave Supersuite|72934|5|Briefly described|p2|Calymmian|Calymmian|Contains inherited zircon magmatic crystallisation ages similar to the Undawidgi and Toolgana Supersuites.|c. 1410 Ma||||Metagabbro and granitic gneisses, with adakitic geochemical affinities.|
79160|Haig Cave Supersuite|72949|6|Mentioned|p40|Ectasian|Calymmian|Madura Province. Represents episodic magmatism with subduction-related, arc-type geochemistry.|c. 1.42-1.39 Ga|||||
79160|Haig Cave Supersuite|73084|4|Described|p: 12, 15, 17, 19, 21, 24, 54, 56, 59...|Calymmian|Calymmian|Madura Province. Series of tholeiitic intrusions formed within an oceanic subduction setting (termed the Loongana Arc; Spaggiari et al., 2015). Interpreted to cover a significant portion of the Madura Province. Dates are from metatonalite veins. Denoted by a strong gravity response. Includes cumulate assemblages. Adakite that intrudes the Pinto Basalt (generally parallel to the main fabric) is not genetically related to said basalt; incorporates inherited zircons from older crustal material (Arid Basin?). [Partly or wholly belongs to the Arubiddy Ophiolite Complex/complex?]. Report includes lithologic/petrographic description, whole-rock geochemistry, geochronology, Sm-Nd, Lu-Hf. [informal gabbros and peridotites from the unit are referred to by location names; not interpreted to reflect specific lithologic units; i.e., Serpent, Loongana, Haig]. Also p: 61-62, 69-70, 78-79, 81, 83-84, 88-89, ~91-100, 112-114, ~118-132, 139-142.|1409 +/- 6 Ma|||Intrudes Pinto Basalt.|Tholeiitic intrusions ranging from hornblende-bearing gabbro to olivine- and pyroxene-bearing peridotites and gabbros. Intruded by dominantly trondhjemitic granites and adakite. Includes pale grey to white, thin leucogranite veins.|
79160|Haig Cave Supersuite|73225|5|Briefly described|p19|||Madura Province. Oceanic arc rocks. Similar age to the Papulankutja Supersuite in Musgrave Province. Appears as Haig Craig Supersuite on p2.|1415-1389 Ma.|||||
35287|Halfway Gneiss|23525|4|Described|p6|Paleoproterozoic|Archean|Intruded by Dumbie Granodiorite. Age: 2550-2000Ma.||||||15-DEC-08
35287|Halfway Gneiss|23527|5|Briefly described|Map Legend|Archean|Archean|||||||07-NOV-08
35287|Halfway Gneiss|23780|5|Briefly described|p49|Paleoproterozoic|Paleoproterozoic|Age: ~2006+/-6 Ma.||||||07-NOV-08
35287|Halfway Gneiss|23781|5|Briefly described|p54|Paleoproterozoic|Archean|Age: c.2540-2000Ma.  Geological Province: Glenburgh Terrane.||||||07-NOV-08
35287|Halfway Gneiss|24544|4|Described|p3, 34-37|Paleoproterozoic|Archean|Age: 2540-2000 Ma. Geological Province: Glenburgh Terrane of Gascoyne Complex. Granitic gneiss. Unconformably overlain by Mount James Formation.||||||07-NOV-08
35287|Halfway Gneiss|50216|5|Briefly described|p206, 211 Fig.4|Paleoproterozoic|Paleoproterozoic|Term used to describe the structurally interleaved segments of the Dalgaringa Supersuite and basement gneiss of the Glenburgh Terrane.||||||07-NOV-08
35287|Halfway Gneiss|50218|5|Briefly described|p240 Fig.2, p242|Paleoproterozoic|Archean|Age: 2550-2000Ma. Geological Province: Glenburgh Terrane (Gascoyne Complex). See also p245, p250.||||||07-FEB-11
35287|Halfway Gneiss|50219|5|Briefly described|p259, p260 Fig. 2|Paleoproterozoic|Archean|Formed by the tectonic interleaving of Dalgaringa Supersuite rocks with late Archaean granitic rocks.  Age: ca. 2550Ma.  Geological Province: Glenburgh Terrane (Gascoyne Complex).||||||07-FEB-11
35287|Halfway Gneiss|50220|5|Briefly described|p280, p281 Fig.1|Paleoproterozoic|Archean|||||||07-NOV-08
35287|Halfway Gneiss|63866|4|Described|p155-p156|Paleoproterozoic|Neoarchean|SHRIMP age derived from Nelson, 2000 and interpreted as the age of igneous crystallization for a granodiorite protolith to the gneiss. Additionally an age of 2550 +/- 7 Ma probably represents the igneous crystallization age of the tonalite protolith to gneiss (Nelson, 2000) while an igneous crystallization age of 2006 +/- 6 Ma is interpreted for a granite protolith (Nelson, 2001). Schists and gneisses of this unit were previously included in the Morrissey Metamorphic Suite.|2554 +/- 5 Ma (SHRIMP U-Pb zircon)|||Intruded by the Dalgaringa Supersuite.|Mafic schist and gneiss, pelitic schist, calc-silicate gneiss, dolomitic marble, metamorphosed granodiorites, tonalites and monzogranites.|
35287|Halfway Gneiss|63869|6|Mentioned|p10|Archean|Archean|Glenburgh Terrane. Basement to Gascoyne Complex.||||||
35287|Halfway Gneiss|64580|4|Described|map legend|Paleoproterozoic|Archean|Interlayered leucocratic and mesocratic granitic gneiss, pale grey granitic gneiss and foliated granite, and gneissic to foliated porphyritic granodiorite.||||||15-DEC-08
35287|Halfway Gneiss|64722|6|Mentioned|Fig. 2 p3-6|Siderian|Neoarchean|Capricorn Orogen?||||||
35287|Halfway Gneiss|65152|5|Briefly described|p1.|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane. c.2000 Ma. Unconformably overlain by Moogie Metamorphics.||||||01-MAY-15
35287|Halfway Gneiss|65830|5|Briefly described|p24, p26 Fig.13|Orosirian|Neoarchean|Formed through the interleaving of the Dalgaringa Supersuite with the Archean basement.|2600-2000 Ma|Of the Gascoyne Complex.||||
35287|Halfway Gneiss|66105|5|Briefly described|Map legend|Proterozoic|Archean|Glenburgh Terrane, Gascoyne Province. 2663-2429 Ma. Interlayered leucocratic and mesocratic granitic gneiss, pale grey granitic gneiss and foliated metagranite, and gneissic to foliated porphyritic metagranodiorite.||||||
35287|Halfway Gneiss|66110|5|Briefly described|Map legend|Proterozoic|Archean|Glenburgh Terrane, Gascoyne Province. Age shown as 2663-2429 Ma. Interlayered leucocratic and mesocratic granitic gneiss, pale grey granitic gneiss and foliated metagranite, and gneissic to foliated porphyritic metagranodiorite.||||||
35287|Halfway Gneiss|66299|4|Described|p1, pp50-56, p192.|Paleoproterozoic|Archean|Component of Glenburgh Terrane, basement to Gascoyne Province. Granitic rocks deformed and metamorphosed to at least amphibolite facies. Extensively intruded by Dumbie Granodiorite, Scrubber Granite, Moorarie and Durlacher Supersuites.|Crystallization ages = c.2663-2429 Ma.|||Interleaved with Moogie Metamorphics and a unit of Moorarie Supersuite. Is overlain by Leake Spring Metamorphics; unconformably overlain by Yilgatherra Formation.|Moderately- to strongly-deformed, variably pegmatite-banded, meso- and leucocratic granitic gneisses.|
35287|Halfway Gneiss|66579|5|Briefly described|Map legend|Paleoproterozoic|Neoarchean|Glenburgh Terrane, Gascoyne Province.|2670-2425 Ma||||Interlayered leucocratic and mesocratic granitic gneiss, pale grey granitic gneiss and foliated metagranite, and gneissic to foliated porphyritic metagranodiorite.|
35287|Halfway Gneiss|66882|6|Mentioned|p116|Neoarchean|Neoarchean|Has similar Nd isotopic traits as, and is a possible source for, Darke Peak Group.|2550 Ma|||||
35287|Halfway Gneiss|66887|4|Described|p1-24|Paleoproterozoic|Archean|Basement in Glenburgh Terrane, southern Gascoyne Province. Age: crystallisation ages of igneous protoliths are between 2555 and 2430 Ma (Kinny et al. 2004; Geological Survey of Western Australia 2009); and numerous inherited zircons, >2600 Ma, and as old as 3447 Ma. Majority (51% of dated magmatic and inherited zircons) of Halfway Gneiss formed between 2600-2430 Ma, mainly through reworking of older gneisses. Old hafnium crustal model ages (3700-3000 Ma) of magmatic zircons, indicate presence of older crustal component up to 3700 Ma. Felsic components of Dalgaringa Supersuite (c. 2000 Ma), interleave with, and have been emplaced during subduction into, Halfway Gneiss. Age distribution of detrital zircons in Mumba Psammite (of Moogie Metamorphics) indicate they were partly derived from underlying Halfway Gneiss. Lithology continued: rock types include interlayered leucocratic granitic gneiss and foliated leucocratic metagranite, mesocratic granitic gneiss, augen gneiss, pegmatite-banded tonalitic and granodioritic gneiss, pale-grey granitic gneiss, gneissic to foliated porphyritic metagranodiorite, foliated metagranite, and metapegmatite. Two mappable units (at 1:100 000 scale) identified: (1) mesocratic granitic gneiss, and (2) leucocratic granitic gneiss and foliated metagranite; rest is undivided.|2555-2430 Ma crystallisation; 3447 Ma inherited|||Tectonic contact with and locally overlain by Moogie Metamorphics. Dalgaringa Supersuite interleaves with, and intrudes, Halfway Gneiss. Moorarie Supersuite granite intrudes mesocratic Halfway Gneiss.|Interlayered granitic gneisses, heterogeneously deformed and metamorphosed to at least amphibolite facies. No sharp boundaries between various rock types interleaved at meso- and megascopic scales. See Comments for detailed lithology.|
35287|Halfway Gneiss|66950|5|Briefly described|p9 Fig.8, p10 Fig.9, p14, p25 Fig.17|Neoarchean|Neoarchean||c. 2660-2430 Ma|||Intruded by the Dalgaringa Supersuite. Unconformably overlain by the Moogie Metamorphics.||
35287|Halfway Gneiss|67247|5|Briefly described|Map legend.|Paleoproterozoic|Archean|Glenburgh Terrane, Gascoyne Province. Has two un-named sub-units mapped separately.|2663 - 2429 Ma.||||Interlayered mesocratic and leucocratic granitic gneiss, pale-grey granitic gneiss and foliated metagranite, and gneissic to foliated porphyritic metagranodiorite.|
35287|Halfway Gneiss|67371|5|Briefly described|Map legend.|Proterozoic|Archean|Glenburgh Terrane, Gascoyne Province. Has two separately-mapped but un-named members; a leucocratic granitic gneiss and foliated leucocratic metagranite, derived from biotite monzogranite and granodiorite; and a mesocratic granitic gneiss, derived from variably porphyritic tonalite.|2663 - 2429 Ma.||||Interlayered leucocratic and mesocratic granitic gneiss, pale grey granitic geniss and foliated metagranite, and gneissic to foliated porphyritic metagranodiorite.|
35287|Halfway Gneiss|67373|5|Briefly described|Map legend.|Proterozoic|Archean|Glenburgh Terrane, Gascoyne Province. |2663 - 2429 Ma.||||Interlayered leucocratic and mesocratic granitic gneiss, pale-grey granitic gneiss and foliated metagranite, and gneissic to foliated porphyritic metagranodiorite.|
35287|Halfway Gneiss|67843|5|Briefly described|Throughout the article.|Paleoproterozoic|Archean|Glenburgh Terrane. Heterogeneously deformed granitic gneisses. Deformation and mineralogy are described in detail.|2660-2430 Ma (Sheppard et al. 2008a).|||Is intruded by Dalgaringa Supersuite. Is unconformably overlain by Moogie Metamorphics/Mumba Psammite.||
35287|Halfway Gneiss|68521|5|Briefly described|Map Legend|Paleoproterozoic|Neoarchean|Another age is also given: 2000 Ma, presumably relating to metamorphism during the Glenburgh Orogeny (2005-1950 Ma).|c.2630-2500 Ma||||Interlayered leucocratic and mesocratic granitic gneiss, pale-grey granitic gneiss and foliated metagranite, and gneissic to foliated porphyritic metagranodiorite.|
35287|Halfway Gneiss|68522|5|Briefly described|Map Legend|Siderian|Neoarchean|Gascoyne Province. |2555-2430 Ma||||Interlayered leucocratic and mesocratic granitic gneiss, pale-grey granitic gneiss and foliated metagranite, and gneissic to foliated porphyritic metagranodiorite.|
35287|Halfway Gneiss|68981|5|Briefly described|p19-20, p23|||Glenburgh Terrane, basement to Gascoyne Province. Hf evolution diagram. Crystallisation history and crustal source of this unit is dissimilar from Pilbara and Yilgarn Cratons, implying the Glenburgh Terrane is exotic to both: discussed.|2555-2430 Ma.||||Granitic gneisses.|
35287|Halfway Gneiss|69003|4|Described|p4, p6-9|||Oldest rocks in the Glenburgh Terrane which forms basement to the southern Gascoyne Province in the Capricorn Orogen. Considered an exotic terrane, juxtaposed during the Ophthalmian and Glenburgh Orogenies. Source of sediments for Moogie Metamorphics psammitic protoliths.|c.2555 - c.2430 Ma (protolith ages).|||Is overlain unconformably by, and in tectonic contact with, Moogie Metamorphics.|Heterogeneous granite gneisses.|
35287|Halfway Gneiss|69011|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Glenburgh Terrane, Gascoyne Province. Mapped as 2 unnamed sub-units.|2555-2125 Ma||||Leucocratic granitic gneiss and foliated leucocratic metagranite, derived from biotite monzogranite and granodiorite; mesocratic granitic gneiss derived from variably porphyritic tonalite.|24-APR-14
35287|Halfway Gneiss|69028|5|Briefly described|Map Legend|Siderian|Neoarchean|Glenburgh Terrane, Gascoyne Province.|2555-2430 Ma||||Interlayered leucocratic and mesocratic granitic gneiss, pale-grey granitic gneiss and foliated metagranite, and gneissic to foliated porphyritic metagranodiorite.|06-MAY-14
35287|Halfway Gneiss|69080|5|Briefly described|p684, p688-689, p694 Fig.9|Siderian|Neoarchean|Oldest component of the Glenburgh Terrane, Gascoyne Province. The gneisses contain abundant inherited zircons, some aged to c.3447 Ma. Their isotopic data indicates the Glenburgh Terrane is exotic, and interpreted to have accreted onto the Pilbara Craton during the 2215-2145 Ma Ophthalmian Orogeny.|2555-2430 Ma.||||Interlayered leucocratic and mesocratic granitic gneiss, pale-grey granitic gneiss and foliated metagranite, and gneissic to foliated porphyritic metagranodiorite.|
35287|Halfway Gneiss|69166|5|Briefly described|geologyp_lut.csv|Paleoproterozoic|Neoarchean|Age derived from gneiss and leucocratic granitic gneiss samples (168947.1.pdf, 185955.1.pdf) Granitic gneiss age is the maximum age of the protolith not of metamorphism.|2006 +/- 6 Ma, 2527  +/-9 Ma (SHRIMP)|||Unconformably overlies Moogie Metamorphics|Interlayered leucocratic and mesocratic granitic gneiss, leucocratic metagranite derived from biotite monzogranite and granodiorite, pale-grey granitic gneiss and foliated metagranite, and gneissic to foliated porphyritic metagranodiorite|
35287|Halfway Gneiss|69237|6|Mentioned|p2|||Gascoyne Province.|2600-2000 Ma.|||||
35287|Halfway Gneiss|69387|5|Briefly described|p3, p6, p12, p15-16, p18, p21-22, p25-35|Siderian|Neoarchean|The basement to the Glenburgh Terrane, Gascoyne Province. Deformations discussed. SG and magnetic susceptibility values given. Gravity and magnetic modelling.|c.2555-2430 Ma (Johnson et al., 2010, 2011).|||Is overlain by Moogie Metamorphics. Is intruded by Dalgaringa Supersuite.|A series of heterogeneous granitic gneisses.|
35287|Halfway Gneiss|69546|5|Briefly described|p102|Paleoproterozoic|Archean|Geological province: Gascoyne Province.|3600-2000 Ma|||||
35287|Halfway Gneiss|69583|5|Briefly described|p130-132, p137, Plate 3|Proterozoic|Proterozoic|Gascoyne Province. Basement to the Glenburgh Terrane.|c.2555-2430 Ma (protoliths).|||Is overlain by Moogie Metamorphics.|Heterogeneous, variably pegmatite-banded, granitic gneisses. Interlayered leucocratic and mesocratic granitic gneiss, pale grey granitic gneiss and foliated metagranite, and gneissic to foliated porphyritic metagranodiorite.|
35287|Halfway Gneiss|69595|5|Briefly described|p19, p32 |Siderian|Neoarchean|Igneous crystallization ages. Reworked basement of the Glenburgh Terrane.|c. 2555 - 2430 Ma|||Intruded by the Dalgaringa Supersuite.|Interlayered granitic gneisses.|
35287|Halfway Gneiss|69596|5|Briefly described|p5-6, p8|Siderian|Neoarchean|Glenburgh Terrane, Gascoyne Province.|2555-2430 Ma.|||Is overlain by the Moogie Metamorphics. Is intruded by Dalgaringa Supersuite.|Heterogeneous granitic gneisses.|
35287|Halfway Gneiss|70019|5|Briefly described|p94|Siderian|Neoarchean|Geological province: Gascoyne Province, Capricorn Orogen. Comprises Neoarchean to Paleoproterozoic basement rock assemblage of the Gascoyne Province.|2555-2430 Ma|||||
35287|Halfway Gneiss|70090|5|Briefly described|p450,453|Paleoproterozoic|Neoarchean|Geological province: Glenburgh Terrane, Gascoyne Province. Crystallisation age of igneous protoliths between 2555-2430 Ma (Johnson et al., 2011a); interpreted to be reworked basement to the Glenburgh Terrane. Magmatic zircon ages similar to Big Red paragneiss, but has distinct Hf isotopic signature from Big Red paragneiss.||||||
35287|Halfway Gneiss|70254|5|Briefly described|p379|||Geological province: Glenburgh Terrane, Yilgarn Craton. Deformed and metamorphosed to at least amphibolite facies (Johnson et al., 2011a). Precursors includes tonalite and gramodiorite, with interpreted protolith ages of 2555-2430 Ma, and inherited zircons with ages between 2600-3447 Ma that record juvenile input during reworking of Archean crust (Johnson et al., 2011a,b, 2013).|||||Mesocratic and leucocratic granitic gneiss.|
35287|Halfway Gneiss|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Neoarchean|Also 2_5m_interpgeop15_lut.csv, 100k_interpgeop_lut.csv, 168947.1.pdf, 185955.1.pdf, West Australian Craton|2555-2429 Ma|||Intruded by Moorarie Supersuite|Interlayered leucocratic and mesocratic granitic gneiss, leucocratic granite, foliated granite, granitic gneiss, gneissic to foliated porphyritic metagranodiorite and pegmatites.|
35287|Halfway Gneiss|70814|5|Briefly described|p34, p59|Paleoproterozoic|Neoarchean|Gascoyne Province.|2555-2430 Ma|||||
35287|Halfway Gneiss|70826|6|Mentioned|p9|Neoarchean|Neoarchean|Gascoyne Province, Glenburgh Terrane.||||||
35287|Halfway Gneiss|71000|6|Mentioned|p64-65|Paleoproterozoic|Archean|Oldest known rocks in the Glenburgh Terrane, southern Gascoyne Province, Capricorn Orogen.|2555-2430 Ma.|||Is overlain unconformably and tectonically by Moogie Metamorphics. Is intruded by Dalgaringa Supersuite.||
35287|Halfway Gneiss|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||felsic gneiss, granite, granodiorite|
35287|Halfway Gneiss|71468|6|Mentioned|p38|||Geological province: Capricorn Orogen, Yilgarn Craton.||||||
35287|Halfway Gneiss|71804|6|Mentioned|p403 fig 10|||Gascoyne Province.||||||
35287|Halfway Gneiss|71869|5|Briefly described|p2-p5, p9, p12-p14, p16-p17, app p1-p2|||Glenburgh Terrane, Capricorn Orogen.|2555-2430 Ma||||Foliated porphyritic biotite granodiorite, biotite tonalite, pegmatite-banded tonalite gneiss and metagranodiorite.|
35287|Halfway Gneiss|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Neoarchean|Glenburgh Terrane, Capricorn Orogen.|Max age 2555+/-4 Ma, min 2429+/-4 Ma.||||Interlayered leucocratic and mesocratic granitic gneiss, pale-grey granitic gneiss and foliated metagranite, and gneissic to foliated porphyritic metagranodiorite.|
35287|Halfway Gneiss|72259|6|Mentioned|p3|Siderian|Neoarchean||ca. 2555-2430 Ma|||||
35287|Halfway Gneiss|73102|5|Briefly described|p3|||Gascoyne Province; Glenburgh Terrane.|||||Interlayered leucocratic and mesocratic granitic gneiss, pale-grey granitic gneiss and foliated metagranite, and gneissic to foliated porphyritic metagranodiorite.|
35287|Halfway Gneiss|73168|5|Briefly described|p758, p764-765|Siderian|Neoarchean|Gascoyne Province, Glenburgh Terrane. Contains an inherited Archean zircon age component at ca 3560-2600 Ma.|2555-2430 Ma|||Interleaved with Moogie Metamorphics.|Granitic gneisses.|
35287|Halfway Gneiss|73214|5|Briefly described|p974 Fig.1|Palaeoproterozoic|Archean|Glenburgh Terrane.||||||
35287|Halfway Gneiss|73442|5|Briefly described|p3|||Gascoyne Province, Glenburgh Terrane.|||||Interleaved leucocratic and mesocratic granitic gneiss, pale-grey granitic gneiss and foliated metagranite, and gneissic to foliated porphyritic metagranodiorite.|
77945|Halfway Well Basalt|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2690 - 2660 Ma (inferred).|Mount White Group|||Basalt; fine grained with local pyroxene-spinifex texture; minor interflow sedimentary rocks; metamorphosed.|
77945|Halfway Well Basalt|71212|5|Briefly described|intro p2|||Yilgarn Craton. ||Mount White Group|||Interlayered basalts and gabbros.|
77945|Halfway Well Basalt|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2692-2662 Ma (inferred)|Unit of Mount White Group.|||Basalt; fine grained with local pyroxene-spinifex texture; minor interflow sedimentary rocks; metamorphosed|
77945|Halfway Well Basalt|73151|5|Briefly described|p2-3, p8, p13.|Neoarchean|Neoarchean|Yilgarn Craton, Kalgoorlie Terrane. Upper part of the Mount White Group, appears conformable with the Vivien Formation. See also Halfway Well Basalt Formation p16.||Mount White Group||Overlies Vivien Formation.|Pillow basalt and gabbro.|
77945|Halfway Well Basalt|73596|6|Mentioned|p1152, 1157-1160, 1162|Neoarchean|Neoarchean|Agnew-Wiluna Greenstone Belt. Co-magmatic with Mount White Dolerite. Ring-plain and submarine aprons surrounding emergent volcanic islands.||Mount White Group.||Conformably overlies Vivien Formation. Is overlain by Maria Mine Formation.|Pillow basalts, co-magmatic gabbro sills.|
27793|Halls Creek Group|505|6|Mentioned|p711|Archean|Archean|Halls Creek Province.|||Includes Olympio Formation.|||
27793|Halls Creek Group|14019|6|Mentioned|p19|||||||||
27793|Halls Creek Group|22440|5|Briefly described|p4|Orosirian|Orosirian|Age 1800- 1840Ma||||||
27793|Halls Creek Group|22496|3|Fully described|p7|Paleoproterozoic|Paleoproterozoic|Redefined to exclude the Ding Dong Downs Volcanics; now comprises Saunders Creek, Biscay and Olympio Formations: on RUBY PLAINS only the latter two represent this group.||||||07-NOV-08
27793|Halls Creek Group|22526|5|Briefly described|P679, P680||Orosirian|||||||
27793|Halls Creek Group|22537|5|Briefly described|34|Proterozoic|Proterozoic|||||||
27793|Halls Creek Group|22547|5|Briefly described|P8||Orosirian|||||||
27793|Halls Creek Group|22661|6|Mentioned|p 313|||||||||
27793|Halls Creek Group|22716|6|Mentioned|p234|||||||||
27793|Halls Creek Group|22741|5|Briefly described|P9, Table3 P19||Proterozoic|||||||
27793|Halls Creek Group|22754|5|Briefly described|p3, p6|||Of the Lamboo Complex.  Age 1880-1840 Ma.  See also p16 and p29.||||||
27793|Halls Creek Group|22764|5|Briefly described|Table 1 p7|Paleoproterozoic|Archean|Includes Olympio Formation.||||||01-FEB-10
27793|Halls Creek Group|22777|5|Briefly described|Map|||||||||
27793|Halls Creek Group|23314|5|Briefly described|329||Paleoproterozoic|||||||07-NOV-08
27793|Halls Creek Group|23323|5|Briefly described|p454 Fig.2|Proterozoic|Proterozoic|In the North Australian Craton.||||||07-FEB-07
27793|Halls Creek Group|23383|1|Redefined|p12, p5 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Lamboo Complex. Comprises: Saunders Creek, Biscay and Olympio Formations. Overlain by Moola Bulla Formation. Intruded by Woodward Dolerite.  Age: 1880 to 1847 Ma.  Geol. Prov: Hooper Orogen.  See also p6 Fig. 3.||||||22-DEC-08
27793|Halls Creek Group|23568|5|Briefly described|p2777 Fig 2|Paleoproterozoic|Paleoproterozoic|Age: ~1915-1845 Ma.||||||07-NOV-08
27793|Halls Creek Group|23599|4|Described|p8|Paleoproterozoic|Paleoproterozoic|Age: c.1880-1850 Ma (SHRIMP U-Pb zircon)||||||07-NOV-08
27793|Halls Creek Group|23601|5|Briefly described| Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Olympio Formation.  Age: c.1860Ma.||||||07-NOV-08
27793|Halls Creek Group|23621|4|Described|p15|Orosirian|Orosirian|See also page 11 table 1. Age: 1880-1845 Ma. Geological Province: Halls Creek Orogen.||||||
27793|Halls Creek Group|23622|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27793|Halls Creek Group|23722|5|Briefly described|p5|Orosirian|Orosirian|Age: c.1880Ma (U-Pb)||||||
27793|Halls Creek Group|23821|5|Briefly described|p245|Proterozoic|Archean|||||||07-NOV-08
27793|Halls Creek Group|23925|5|Briefly described|p234 Fig. 13|Orosirian|Orosirian|Age: 1915-1845 Ma.  Geological Province: Halls Creek Orogen.||||||
27793|Halls Creek Group|24173|5|Briefly described|p15|Paleoproterozoic|Paleoproterozoic|Includes Saunders Creek, Biscay and Olympio Formations. Unconformably overlies Ding Dong Downs Volcanics. Geological Province: Halls Creek Orogen. Age: ~1880-1845Ma.||||||07-NOV-08
27793|Halls Creek Group|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Lamboo Complex (central zone).||||||07-NOV-08
27793|Halls Creek Group|24572|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: >1835Ma.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
27793|Halls Creek Group|29447|6|Mentioned|p11|||||||||
27793|Halls Creek Group|29805|6|Mentioned|p7|||||||||
27793|Halls Creek Group|29807|6|Mentioned|p6|||See also P15||||||
27793|Halls Creek Group|29809|6|Mentioned|Table 1|||||||||
27793|Halls Creek Group|29813|4|Described|Table 2|||||||||
27793|Halls Creek Group|29818|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
27793|Halls Creek Group|29845|6|Mentioned|p108|||||||||
27793|Halls Creek Group|30097|6|Mentioned|Table 23|||Also Table 25||||||
27793|Halls Creek Group|30525|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27793|Halls Creek Group|30526|6|Mentioned|p110|||||||||
27793|Halls Creek Group|30533|3|Fully described|p9|||On Table 1. Age 2700 m.y. (uncertain)||||||
27793|Halls Creek Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
27793|Halls Creek Group|30892|3|Fully described|p93|||? Archaean age. See also pp94-100.||||||25-SEP-06
27793|Halls Creek Group|30893|5|Briefly described|p205|||Archaean age. Lithology||||||
27793|Halls Creek Group|30894|5|Briefly described|p250|||Archaean to Lower Proterozoic||||||
27793|Halls Creek Group|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27793|Halls Creek Group|30896|4|Described|p9|||Archaean age||||||
27793|Halls Creek Group|30897|4|Described|p8|||Stratigraphy||||||
27793|Halls Creek Group|30898|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27793|Halls Creek Group|31226|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
27793|Halls Creek Group|31230|6|Mentioned|p182|||||||||
27793|Halls Creek Group|31361|6|Mentioned|p4|||||||||
27793|Halls Creek Group|31362|6|Mentioned|p7|||Correlated||||||
27793|Halls Creek Group|31393|6|Mentioned|Pl.25|||||||||
27793|Halls Creek Group|32171|6|Mentioned|p5|||Refers Dow & Gemuts (1969)||||||
27793|Halls Creek Group|32643|6|Mentioned|p535|||||||||
27793|Halls Creek Group|32659|6|Mentioned|Map legend|Paleoproterozoic|Archean|Archaean or Lower Proterozoic||||||07-NOV-08
27793|Halls Creek Group|32660|4|Described|Table 1|||Re stratigraphy||||||
27793|Halls Creek Group|32664|6|Mentioned|Map legend|Proterozoic|Archean|Archaean or Proterozoic. Briefly described in notes||||||07-NOV-08
27793|Halls Creek Group|32699|5|Briefly described|Map legend|Archean|Archean|Slate, green schist, mica schist and andalusite schist.||||||07-NOV-08
27793|Halls Creek Group|32701|5|Briefly described|Table 1|||||||||
27793|Halls Creek Group|32728|4|Described|p19|||||||||
27793|Halls Creek Group|33376|6|Mentioned|Map legend|Proterozoic|Archean|Archaean and/or Proterozoic||||||07-NOV-08
27793|Halls Creek Group|33377|6|Mentioned|Table 1|||Stratigraphy||||||
27793|Halls Creek Group|33443|6|Mentioned|p260|||||||||
27793|Halls Creek Group|34604|6|Mentioned|Fig.4|||||||||
27793|Halls Creek Group|34684|6|Mentioned|p102|||||||||
27793|Halls Creek Group|34723|6|Mentioned|p239|||||||||
27793|Halls Creek Group|35040|6|Mentioned|p375|||||||||
27793|Halls Creek Group|35120|6|Mentioned|Map legend|Paleoproterozoic|Archean|Archaean - Proterozoic||||||07-NOV-08
27793|Halls Creek Group|35495|6|Mentioned|p340|||||||||
27793|Halls Creek Group|35726|6|Mentioned|p69|||||||||
27793|Halls Creek Group|35950|6|Mentioned|p302|||||||||
27793|Halls Creek Group|36225|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27793|Halls Creek Group|36257|6|Mentioned|p27|||||||||
27793|Halls Creek Group|36308|6|Mentioned|p211|||||||||
27793|Halls Creek Group|36473|6|Mentioned|Map legend|Proterozoic|Archean|Archaean to Proterozoic||||||07-NOV-08
27793|Halls Creek Group|36532|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27793|Halls Creek Group|36551|6|Mentioned|p22|||Also mentioned p25,P41, p115.||||||25-SEP-06
27793|Halls Creek Group|36885|3|Fully described|p165|||||||||
27793|Halls Creek Group|36887|6|Mentioned|p206|||Formerly Halls Creek Metamorphics.||||||25-SEP-06
27793|Halls Creek Group|36898|6|Mentioned|p183|||||||||
27793|Halls Creek Group|36902|6|Mentioned|p11|||||||||
27793|Halls Creek Group|37299|6|Mentioned|Fig.1|||||||||
27793|Halls Creek Group|37462|3|Fully described|p221|||||||||
27793|Halls Creek Group|37577|6|Mentioned|p26|||||||||
27793|Halls Creek Group|38066|6|Mentioned|Fig.9|||P53||||||
27793|Halls Creek Group|38482|6|Mentioned|Table 1|||||||||
27793|Halls Creek Group|39827|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27793|Halls Creek Group|39887|6|Mentioned|p453|||||||||
27793|Halls Creek Group|39889|6|Mentioned|p495|||||||||
27793|Halls Creek Group|40494|4|Described|p5|||Also mention on p3.||||||25-SEP-06
27793|Halls Creek Group|40765|6|Mentioned|p3|||||||||
27793|Halls Creek Group|40793|6|Mentioned|p165|||||||||
27793|Halls Creek Group|41125|6|Mentioned|p30|||||||||
27793|Halls Creek Group|41158|6|Mentioned|p18|||||||||
27793|Halls Creek Group|41465|5|Briefly described|p4|||||||||
27793|Halls Creek Group|41635|6|Mentioned|p19|||||||||
27793|Halls Creek Group|41883|6|Mentioned|p65|||||||||
27793|Halls Creek Group|41952|6|Mentioned|p188|||||||||
27793|Halls Creek Group|41976|5|Briefly described|p453|||||||||
27793|Halls Creek Group|41977|4|Described|p471|||||||||
27793|Halls Creek Group|41987|6|Mentioned|p70|||||||||
27793|Halls Creek Group|42149|6|Mentioned|p703|||||||||
27793|Halls Creek Group|42326|5|Briefly described|p9|||||||||
27793|Halls Creek Group|42329|6|Mentioned|Fig.2 P6|||||||||
27793|Halls Creek Group|42504|6|Mentioned|p59|||||||||
27793|Halls Creek Group|42730|5|Briefly described|p19|||||||||
27793|Halls Creek Group|42768|5|Briefly described|p6, Fig.6|||||||||
27793|Halls Creek Group|42811|6|Mentioned|p5|||||||||
27793|Halls Creek Group|42814|6|Mentioned|p5|||||||||
27793|Halls Creek Group|43299|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
27793|Halls Creek Group|43303|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
27793|Halls Creek Group|43561|6|Mentioned|p1437|||||||||
27793|Halls Creek Group|43595|4|Described|p74,223,349|||Accumulate approx. 2150 Ma cease approx.1920 Ma||||||
27793|Halls Creek Group|43631|6|Mentioned|p7,9|||of East Kimberley||||||
27793|Halls Creek Group|43632|6|Mentioned|p2||Proterozoic|||||||
27793|Halls Creek Group|43666|6|Mentioned|p52,Table 2||Neoproterozoic|||||||
27793|Halls Creek Group|43794|5|Briefly described|p319||Proterozoic|||||||
27793|Halls Creek Group|43819|6|Mentioned|p33|||||||||
27793|Halls Creek Group|43854|5|Briefly described|Map Legend||Proterozoic|||||||
27793|Halls Creek Group|44155|4|Described|p232-255|Paleoproterozoic|Paleoproterozoic|Matheson and Guppy (1949), Dow and Gemuts (1969). All basalts in this unit are tholeiitic, more-iron-rich than Antrim Plateau Volcanics in the same region.|||Ding Dong Downs Volcanics; Saunders Creek, Biscay, Olympio Formations.|Equivalent to Tickalara Metamorphics. Intruded by Woodward Dolerite.|Undivided: phyllitic siltstone and greywacke, schist; some acid volcanics.|
27793|Halls Creek Group|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes: Saunders Creek, Biscay and Olympio Formations. Age: c. 1855Ma and 1880Ma.  In the Lamboo Complex (eastern zone).||||||07-NOV-08
27793|Halls Creek Group|44317|14|Not recorded|p.5||Proterozoic|||||||
27793|Halls Creek Group|44318|14|Not recorded|map legend|||Archaean or Proterozoic.||||||
27793|Halls Creek Group|44324|14|Not recorded|p.5|||Fig.2, Tb.1. (Archaean or Proterozoic).||||||
27793|Halls Creek Group|44325|14|Not recorded|map legend|||Archaean or Proterozoic.||||||
27793|Halls Creek Group|44363|4|Described|p.8,9|||Archaean or Lower Proterozoic.||||||
27793|Halls Creek Group|44364|14|Not recorded|map legend|||||||||
27793|Halls Creek Group|44366|14|Not recorded|p.8, Table 1|||Includes Olympio Formation. Archaean or Proterozoic.||||||
27793|Halls Creek Group|44367|14|Not recorded|map legend|||(Reprinted 1971).||||||
27793|Halls Creek Group|44397|14|Not recorded|p.9,18, Fig.4,Tb.1|||Archaean or Proterozoic.||||||
27793|Halls Creek Group|44398|14|Not recorded|map legend|||Archaean or Proterozoic.||||||
27793|Halls Creek Group|44693|5|Briefly described|Map Legend||Proterozoic|||||||
27793|Halls Creek Group|44694|5|Briefly described|Map Legend||Proterozoic|||||||
27793|Halls Creek Group|44868|5|Briefly described|Map Legend||Proterozoic|||||||
27793|Halls Creek Group|45047|2|Defined|p61|Archean|Archean|Prob. Archaean||||||07-NOV-08
27793|Halls Creek Group|45048|5|Briefly described|p10|||Lithology of units||||||
27793|Halls Creek Group|45112|5|Briefly described|Table 4|||||||||
27793|Halls Creek Group|45140|2|Defined|p12-15, p17, p25, p42, p58, p60, p73|||See also Appx.p2, p11-12. Dow and Gemuts (1969). Formerly Halls Creek Metamorphics (Traves, 1955). Named after Halls Creek township. Halls Creek Province. Probably several thousand metres thick. Low-grade metamorphism dated at 1961 +/- 27 Ma (Dow and Gemuts, 1969). Probable maximum age is 2200 Ma (Page, 1976).|>1960 Ma.||Ding Dong Downs Volcanics; Saunders Creek, Biscay, Olympio Formations.|Correlated with the Tanami and Arunta Complexes.|Tightly-folded low-grade metasediments and metavolcanics.|
27793|Halls Creek Group|46797|5|Briefly described|p79|||Age||||||
27793|Halls Creek Group|46864|4|Described|p39|||||||||
27793|Halls Creek Group|46899|6|Mentioned|p8|||Thermal conductivity||||||
27793|Halls Creek Group|48927|6|Mentioned|p10|||||||||
27793|Halls Creek Group|48931|3|Fully described|p9|||||||||
27793|Halls Creek Group|48938|4|Described|p8|||Lithology.||||||
27793|Halls Creek Group|48950|6|Mentioned|p8|||||||||
27793|Halls Creek Group|50437|6|Mentioned|p5.1|||Intrudes: Saunders Creek Formation.||||||
27793|Halls Creek Group|60006|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Halls Creek Orogen. Unconformably overlain by Whitewater Volcanics and Bucket Spring Member. Schist, phyllite, volcanics, slate||||||07-NOV-08
27793|Halls Creek Group|60283|6|Mentioned|p25 Fig.2|||Halls Creek Orogen.||||||
27793|Halls Creek Group|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Lambo Complex (Eastern Zone). Includes: Biscay Formation, Olympio Formation.||||||
27793|Halls Creek Group|60682|4|Described|piii|Paleoproterozoic|Paleoproterozoic|Ferruginous phyllite, quartz-mica schist, mylonitised acid volcanics, quartz-sericite schist and slate. Age: >1800Ma. Geological Province: Halls Creek Orogen.||||||07-NOV-08
27793|Halls Creek Group|60724|1|Redefined|p4, p6|||Proposed the group be redefined to exclude all rocks below unconformity at base of Saunders Creek Fm, including Sophie Downs Granite and Ding Dong Downs Volcs (both prev.mapped within the group). Revision to incl: Saunders Creek, Biscay and Olympio Fms.||||||
27793|Halls Creek Group|61861|6|Mentioned|Fig.2.|||Correlative with Tanami Group.|||Includes Saunders Creek, Biscay and Olympio Formations.|||
27793|Halls Creek Group|63866|5|Briefly described|p105, p130, p137|||Litchfield Province, Pine Creek Orogen. |||Includes the Saunders Creek Formation, Biscay Formation and the Olympio Formation.|Overlies the Ding Dong Downs Volcanics. Intruded by the Woodward Dolerite.||
27793|Halls Creek Group|64104|6|Mentioned|p63 Fig.1|Paleoproterozoic|Paleoproterozoic||||Includes Olympio Formation.|||
27793|Halls Creek Group|64329|5|Briefly described|p15|||Contains the informally named "Niobium Tuff" which hosts the Brockman deposit.||||||
27793|Halls Creek Group|64572|6|Mentioned|p802 Fig. 4, p803 Fig. 5|Paleoproterozoic|Paleoproterozoic|Age: 1915-1845Ma. Geological Province: North Australian Craton.||||||22-DEC-08
27793|Halls Creek Group|64580|6|Mentioned|map legend|||||||||
27793|Halls Creek Group|64722|5|Briefly described|Fig. 2 p3-6, p9, 24|Orosirian|Orosirian|Of Halls Creek / Leopold orogen. Inferred to have accumulated on the conjugate passive margin to the proto-North Australian Craton to the east.|~1890-1850 Ma.|||Unconformably overlies Ding Dong Downs Volcanics.||11-APR-12
27793|Halls Creek Group|64731|5|Briefly described|p164, 165|Paleoproterozoic|Paleoproterozoic|High-level bimodal volcanism.|1855 Ma.|||||12-APR-12
27793|Halls Creek Group|64956|6|Mentioned|p96, p97|||||||||07-FEB-11
27793|Halls Creek Group|65331|5|Briefly described|Map legend + overview geology map legend|Palaeoproterozoic|Palaeoproterozoic|Of Halls Creek Orogen. Schist, undifferentiated ferruginous phyllite, altered volcanics, slate||||||
27793|Halls Creek Group|66845|5|Briefly described|p536 Fig.2, p537|Paleoproterozoic|Paleoproterozoic|Eastern zone of Lamboo Complex. Rests unconformably on granite and volcanic rock dated at c. 1910 Ma (Tyler et al. 1995; Blake et al. 2000).|c. 1880-1845 Ma|||||
27793|Halls Creek Group|68078|6|Mentioned|p2, p5|Paleoproterozoic|Paleoproterozoic|Deposited on granitic and volcanic basement of Ding Dong Downs Volcanics.|1845-1880 Ma||||Sedimentary and volcanic rocks.|
27793|Halls Creek Group|68244|6|Mentioned|p664,666|||||||Overlain unconformably by Landrigan Formation (Kuniandi Group).||21-JUN-19
27793|Halls Creek Group|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleoproterozoic|Paleoproterozoic|See also 100k_maginterpgeop_lut.csv. Lamboo Complex. Variably magnetic.|1910-1840 Ma (Tyler, 2000).||Includes Olympio Formation.||Metasedimentary and igneous rock; mafic volcanic rock.|
27793|Halls Creek Group|69003|4|Described|p19, p20 Fig.25|Paleoproterozoic|Paleoproterozoic|E zone, Lamboo Province, Halls Creek Orogen.|c.1880-c.1845 Ma.||Saunders Creek, Biscay, Olympio Formations.|Overlies Ding Dong Downs Volcanics and Sophie Downs Suite.|Sedimentary and volcanic rocks.|
27793|Halls Creek Group|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Metamorphic age 1861 +/-5 Ma SHRIMP.|||Includes Olympio Formation, Biscay Formation, Saunders Creek Formation, and unnamed unit.||Pelite, psammite, with basaltic and andesitic to trachytic metavolcanic and metavolcaniclastic rock|31-JUL-15
27793|Halls Creek Group|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv, GA_geochron.csv. |1861 Ma||Includes Olympio Formation, Biscay Formation, Saunders Creek Formation||Undivided; pelite, psammite with basaltic and andesitic to trachytic metavolcanic and metavolcaniclastic rock.|
27793|Halls Creek Group|69422|6|Mentioned|p7:1|||Eastern Zone, Halls Creek Orogen.||||||12-JUL-16
27793|Halls Creek Group|69452|6|Mentioned|p36:6|||Halls Creek Orogen.||||Is overlain unconformably by Kellys Knob Sandstone.||12-JUL-16
27793|Halls Creek Group|69585|5|Briefly described|p2, p4|Orosirian|Orosirian||1880-1845 Ma.||Saunders Creek, Biscay, Olympio Formations.|Unconformably overlies Ding Dong Downs Volcanics.|Metasedimentary and volcanic rocks.|
27793|Halls Creek Group|69587|4|Described|GEOL_LUT_CSV files|||Geological Province: Lamboo Province, Halls Creek Orogen. See 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|||Includes Biscay Formation, Olympio Formation.|||
27793|Halls Creek Group|69597|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|Eastern Lamboo Province. Deposited on the passive continental margin of the North Australia Craton. |1910-1845 Ma||||Mafic volcanic rocks.|
27793|Halls Creek Group|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|1907-1808 Ma (Inferred)||Includes Olympio Formation, Saunders Creek Formation.||Migmatitic pelitic hornfels comprising quartz-K-feldspar-biotite-cordierite-sillimanite; locally retrogressed to quartz-muscovite-biotite-chlorite(-sillimanite)-andalusite schist|
27793|Halls Creek Group|70154|4|Described|100k_interpgeol_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv.|1808-1907 Ma||Olympio Formation||Migmatitic pelitic hornfels comprising quartz, k feldspar, biotite, cordierite and sillimanite.  locally retrogressed to quartz-muscovite-biotite-chlorite(-sillimanite)-andalusite schist.|
27793|Halls Creek Group|70206|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic||||||Ferruginous phyllite, schist, altered volcanic rocks and slate.|
27793|Halls Creek Group|70731|5|Briefly described|p269-270,272-273,277-278|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.|1880-1847 Ma||Includes Olympio and Biscay formations.|||
27793|Halls Creek Group|70812|4|Described|p5, p7, p9, p11-p12, p19, p25, p38|Orosirian|Orosirian|Eastern Zone of the Halls Creek Orogen, Lamboo Province. Hosts signifcant mineral deposits and occurences which are described.|1880-1847 Ma||Includes the Saunders Creek Formation, Biscay Formation and Olympio Formation and the Ding Dong Downs Volcanics.|Unconformably overlies the Ding Dong Downs Volcanics. Intruded by the Woodward Dolerite.|Siliciclastic sedimentary and volcanic rocks.|
27793|Halls Creek Group|70826|6|Mentioned|p5 tbl 2, p9|Paleoproterozoic|Paleoproterozoic|Halls Creek Basin.||||||22-APR-20
27793|Halls Creek Group|70851|4|Described|p3-p5, p18-p19, p23-p24, p28-p29|Paleoproterozoic|Paleoproterozoic|Eastern Zone, Lamboo Province.|c. 1880-1847 Ma||Includes the Saunders Creek Formation, Biscay Formation and the Olympio Formation.|Unconformably overlies the Sophie Downs Suite and Ding Dong Downs Volcanics. Intruded by the Woodward Dolerite.|Siliciclastic sedimentary and volcanic rocks.|
27793|Halls Creek Group|71113|5|Briefly described|p97-98, p109|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen.|1880-1840 Ma||Includes Olympio Formation, Biscay Formation and Saunders Creek Formation.|||21-AUG-19
27793|Halls Creek Group|71140|5|Briefly described|p97-98, 101, 109-110|Orosirian|Orosirian|Eastern Zone, Lamboo Province, Halls Creek Orogen.|1880-1840 Ma.||Saunders Creek, Biscay, Olympio Formations.|Is intruded by sills of Woodward Dolerite.|Low- to medium-grade metasedimentary and meta-igneous rocks.|
27793|Halls Creek Group|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv, 100k_interpgeol_lut.csv and geochron files.|1880-1845 Ma||Includes Biscay Formation, Brim Rockhole Formation, Olympio Formation, Saunders Creek Formation.|Underlain by Sophie Downs Suite.|Pelite and psammite with basaltic and andesitic to trachytic metavolcanic and metavolcaniclastic rock|
27793|Halls Creek Group|71281|4|Described|p422|||Eastern Zone, Lamboo Province. Greenschist to lower amphibolite facies metasedimentary and metavolcanic rocks. Folded during the 1835-1810 Ma Halls Creek Orogeny.|||Olympio Formation.|Is intruded by the Sally Downs Supersuite.|Basal sandstones with c.1881 Ma mafic volcanic rocks, overlain by metaturbidites containing intercalated active-margin alkaline volcanic rocks.|
27793|Halls Creek Group|71397|4|Described|p1-6,8,14,33,42,48|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen. Exposed in a >275 km long, NNE-trending belt of greenschist facies metasedimentary and metavolcanic rocks. Marks new depositional phase in the Eastern Zone after basement development. Mylonites in the Halls Creek Group likely associated with c. 1000-800 Ma Yampi Orogeny (Tyler and Griffin, 1990; Tyler et al., 1995).|||Includes Olympio Formation, Biscay Formation, Brim Rockhole Formation, Saunders Creek Formation.|Underlain unconformably by Sophie Downs Suite. Intruded by Woodward Dolerite.||28-NOV-19
27793|Halls Creek Group|71873|5|Briefly described|p427|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province. Intruded by Woodward Dolerite during Halls Creek Orogeny c. 1832-1808 Ma.|||Includes Olympio, Biscay, Brim Rockhole and Saunders Creek formations.|Underlain unconformably by Sophie Downs Suite.||
27793|Halls Creek Group|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Halls Creek Orogen.|||||Pelite and psammite with basaltic and andesitic to trachytic metavolcanic and metavolcaniclastic rock.|
27793|Halls Creek Group|72437|6|Mentioned|p7, p11, p24|||||||Intruded by the San Sou suite.||
27793|Halls Creek Group|73089|5|Briefly described|p24-28, p31, p37, p43|Orosirian|Orosirian|Lamboo Province, Eastern Zone. Kimberley region. Comparable to the Tanami Group in terms of lithostratigraphy, changes in provenance and thickness.|1885-1835 Ma|||||
40171|Hamelin Granite|24542|5|Briefly described|p7, 28|Neoproterozoic|Mesoproterozoic|Of Leeuwin Complex. Granite gneisses.||||||20-NOV-08
40171|Hamelin Granite|24595|5|Briefly described|p588|||Of Myers (1998).  Part of the Leeuwin Complex.  Previously referred to as Dunsborough Suite (Kay, 1958).  Surrounds the Cowaramup Gneiss.  Geological Province: Leeuwin Block.||||||
68611|Hamersley Group, lower|50216|6|Mentioned|p209|||Informal - see Hamersley Group.||||||
68611|Hamersley Group, lower|69185|5|Briefly described|500k_geologyp08_lut.csv||Neoarchean|Geological Province: Pilbara Craton.|||Includes Carawine Dolomite, Marra Mamba Iron Formation, Wittenoom Formation.|||
68611|Hamersley Group, lower|70826|6|Mentioned|p6 tbl 2, p8|Paleoproterozoic|Neoarchean|Hamersley Basin, Pilbara Craton.||Mount Bruce Supergroup|Pinjian Chert Breccia, Mount McRae Shale|||26-SEP-17
68611|Hamersley Group, lower|72034|6|Mentioned|500k_interpgeop16_lut|Neoarchean|Neoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Marra Mamba Iron Formation, Mount McRae Shale, Mount Sylvia Formation, Wittenoom Formation, Carawine Dolomite.|||
80096|Hamersley Group, upper|69185|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological Province: Pilbara Craton.|||Includes Boolgeeda Iron Formation, Brockman Iron Formation, Weeli Wolli Formation, Woongarra Rhyolite.|||
80096|Hamersley Group, upper|70826|6|Mentioned|p6 tbl 2, p9|Paleoproterozoic|Paleoproterozoic|Hamersley Basin.||Mount Bruce Supergroup||Conformably overlain by the Turee Creek Group.||
80096|Hamersley Group, upper|72034|6|Mentioned|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Boolgeeda Iron Formation, Woongarra Rhyolite, Weeli Wolli Formation, Brockman Iron Formation.|||
33838|Hamersley Range Megasequence|22546|6|Mentioned|371|||Geol province Turee Creek Basin||||||
77858|Hampton Hill Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2726 -2680 Ma (inferred).|Coolgardie Subgroup||Overlies Lindsays Basalt|Komatiite and subordinate basalt that may have spinifex texture or be pillowed, peridotite; metamorphosed.|
77858|Hampton Hill Formation|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).  See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2726-2680 Ma (inferred)|Unit of Coolgardie Subgroup.|||Komatiite, basalt: variolitic, spinifex-textured, komatiitic, pillowed, metamorphosed; pyroxenite, peridotite, ultramafic schist; includes talc-chlorite(-carbonate) and tremolite-chlorite schist.|
77858|Hampton Hill Formation|73596|6|Mentioned|p1162|||Coolgardie Inlier, Kalgoorlie Terrane.||Coolgardie Subgroup.||Overlies Lindsays Basalt. Is overlain by Gleesons Basalt.||
25940|Hampton Sandstone|14227|5|Briefly described|Enclos. 2|Late Eocene|Middle Eocene|Presented as Princess Royal Spongolite, Hampton SS.||||||07-FEB-11
25940|Hampton Sandstone|22587|6|Mentioned|p79 Fig.7|Late Eocene|Middle Eocene|||||||
25940|Hampton Sandstone|22613|4|Described|p20|Late Eocene|Middle Eocene|||||||
25940|Hampton Sandstone|22614|5|Briefly described|map|Eocene|Eocene|||||||
25940|Hampton Sandstone|22626|6|Mentioned|439 fig 3|Eocene|Eocene|Geol province Eucla Basin. Max thickness 85 m.  Overlying unit Wilson Bluff Limestone.||||||21-OCT-08
25940|Hampton Sandstone|23138|5|Briefly described|p240|||||||||
25940|Hampton Sandstone|23331|5|Briefly described|1089 Fig.2|Middle Eocene|Middle Eocene|||||||
25940|Hampton Sandstone|23488|5|Briefly described|p36, p38 Fig. 3|Eocene|Eocene|Overlies the Paling Member.  Geological Province: Eucla Basin.||||||
25940|Hampton Sandstone|23533|5|Briefly described|p564 Fig 3|Middle Eocene||Geological Province: Bremer Basin.||||||
25940|Hampton Sandstone|23582|5|Briefly described|Map Legend|Eocene|Eocene|Of Eundynie Group. Poorly sorted sandstone, typically quartz rich; includes subordinate gravel, conglomerate and siltstone.||||||27-JUN-06
25940|Hampton Sandstone|23584|5|Briefly described|p29|Late Eocene|Eocene|Of Eundynie Group. Geological Province: Yilgarn Craton.||||||
25940|Hampton Sandstone|23989|5|Briefly described|p56|Late Eocene|Early Eocene|Geological Province: Yilgarn Craton. See also misspelt Hampton Formation in this paper.||||||03-MAR-10
25940|Hampton Sandstone|24057|5|Briefly described|p97|Tertiary|Tertiary|Geological Basin: Eucla Basin.||||||
25940|Hampton Sandstone|24094|6|Mentioned|p271|||Geological Province: Eucla Basin||||||16-MAR-05
25940|Hampton Sandstone|24324|5|Briefly described|p27|Early Eocene|Late Paleocene|Geological Province: Eucla Basin||||||
25940|Hampton Sandstone|24347|5|Briefly described|p121|Middle Eocene|Middle Eocene|Overlying unit: Wilson Bluff Limestone. Maximum thickness 30m.||||||27-JUL-09
25940|Hampton Sandstone|24396|5|Briefly described|p222 Fig.5, p228|Eocene|Eocene|Age: 41-42Ma.  Marine clastics.  Geological Province: Eucla Basin.||||||
25940|Hampton Sandstone|24397|4|Described|p237|||No longer includes Khasta Member (rocks). Overlain by Wilson Bluff Limestone. Geological Province: Eucla Basin.||||||27-JUL-09
25940|Hampton Sandstone|24606|5|Briefly described|p956|Tertiary|Tertiary|Conformably overlain by the Wilson Bluff Limestone. Geological Province: Eucla Basin.||||||
25940|Hampton Sandstone|24617|6|Mentioned|p115 Fig. 3|Eocene|Eocene|Geological Province: Eucla Basin.||||||
25940|Hampton Sandstone|30012|4|Described|Table 1|||||||||
25940|Hampton Sandstone|30268|6|Mentioned|p44|||||||||
25940|Hampton Sandstone|30563|4|Described|p11|||Table on P7||||||
25940|Hampton Sandstone|30564|5|Briefly described|p11|||||||||
25940|Hampton Sandstone|30945|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
25940|Hampton Sandstone|30975|6|Mentioned|Map legend|late Eocene|late Eocene|||||||
25940|Hampton Sandstone|31562|5|Briefly described|p13|||Stratigraphic table P10.||||||
25940|Hampton Sandstone|31850|3|Fully described|p33|||Summary of definition.||||||
25940|Hampton Sandstone|31902|4|Described|Table 1|||Fig.1||||||
25940|Hampton Sandstone|31903|6|Mentioned|Map legend|Tertiary|Tertiary|Section only||||||
25940|Hampton Sandstone|31904|4|Described|p7|||Refers Lowry (1968). See also Table 1||||||
25940|Hampton Sandstone|31906|5|Briefly described|p7|||Refers Lowry (1968). Table 1||||||
25940|Hampton Sandstone|31907|4|Described|p7|||See also Table 1, Fig.1||||||
25940|Hampton Sandstone|31908|4|Described|Table 1|||M.-U.Eocene||||||
25940|Hampton Sandstone|31909|3|Fully described|p7|||Formerly "Hampton Conglomerate".||||||27-JUN-06
25940|Hampton Sandstone|31913|4|Described|Table 1|||P10||||||
25940|Hampton Sandstone|31915|6|Mentioned|Map legend|Eocene|Eocene|||||||
25940|Hampton Sandstone|32117|6|Mentioned|Fig.2|||||||||
25940|Hampton Sandstone|32552|2|Defined|p10|middle Eocene|middle Eocene|See also P11, 37, 53 etc.||||||
25940|Hampton Sandstone|32648|6|Mentioned|p32|||Eocene||||||
25940|Hampton Sandstone|32750|5|Briefly described|p304|||Distribution||||||
25940|Hampton Sandstone|33589|5|Briefly described|p10|||See also P11. U.Eocene.||||||
25940|Hampton Sandstone|33595|6|Mentioned|p6|||||||||
25940|Hampton Sandstone|34192|6|Mentioned|Map legend|Oligocene|Eocene|Lower Miocene - Eocene||||||
25940|Hampton Sandstone|34194|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
25940|Hampton Sandstone|34308|6|Mentioned|Fig.97|||Eocene||||||
25940|Hampton Sandstone|34344|6|Mentioned|p3|||Middle Eocene||||||
25940|Hampton Sandstone|34742|6|Mentioned|Map legend|late Eocene|late Eocene|||||||
25940|Hampton Sandstone|35496|4|Described|Table 1|||Also on P21||||||
25940|Hampton Sandstone|35772|6|Mentioned|p9|||||||||
25940|Hampton Sandstone|36257|6|Mentioned|Table 2.1|||||||||
25940|Hampton Sandstone|36890|3|Fully described|p413|||Formerly Hampton Conglomerate.||||||21-OCT-08
25940|Hampton Sandstone|36902|6|Mentioned|p24|||||||||
25940|Hampton Sandstone|36915|6|Mentioned|Fig.6|||||||||
25940|Hampton Sandstone|38482|6|Mentioned|p24|||See also Table 11.||||||
25940|Hampton Sandstone|39923|6|Mentioned|p354|||||||||
25940|Hampton Sandstone|40003|5|Briefly described|Table 14|||See also Fig.16||||||
25940|Hampton Sandstone|40429|6|Mentioned|Fig.2|||||||||
25940|Hampton Sandstone|41626|6|Mentioned|p46|||||||||
25940|Hampton Sandstone|42086|5|Briefly described|Fig.2 P4|||||||||
25940|Hampton Sandstone|42108|3|Fully described|p323|||||||||
25940|Hampton Sandstone|42265|5|Briefly described|p2|Early Oligocene|Middle Eocene|Terrestrial and marine sequence.||||||13-AUG-08
25940|Hampton Sandstone|42356|5|Briefly described|Fig.15 P119|late Eocene|middle Eocene|See also Microfiche 7 p15, Fig.4, Fig.9, 10, 12, 13.||||||
25940|Hampton Sandstone|42475|6|Mentioned|p20|||||||||
25940|Hampton Sandstone|42535|5|Briefly described|p17|||Eucla Basin||||||
25940|Hampton Sandstone|42545|6|Mentioned|Fig.3 P10|||||||||
25940|Hampton Sandstone|42734|5|Briefly described|map legend|Tertiary||||||||
25940|Hampton Sandstone|42816|3|Fully described|p22|||||||||
25940|Hampton Sandstone|42862|5|Briefly described|p8|||||||||
25940|Hampton Sandstone|42959|5|Briefly described|p57|||see also p58 Fig.3||||||
25940|Hampton Sandstone|43040|5|Briefly described|Fig.2,p861|||||||||
25940|Hampton Sandstone|43053|5|Briefly described|Map Legend|Eocene|Paleocene|Marine sand. Geological Province: Eucla Basin.||||||25-MAY-05
25940|Hampton Sandstone|43065|5|Briefly described|Fig.5,p92|||||||||
25940|Hampton Sandstone|43258|5|Briefly described|Map Legend|Eocene|Paleocene|||||||
25940|Hampton Sandstone|43280|6|Mentioned|Map Legend||Tertiary|||||||
25940|Hampton Sandstone|43298|5|Briefly described|Map Legend|Eocene|Paleocene|||||||
25940|Hampton Sandstone|43498|6|Mentioned|8||Middle Eocene|||||||
25940|Hampton Sandstone|43658|6|Mentioned|p4||Early Eocene|||||||
25940|Hampton Sandstone|43667|6|Mentioned|Fig.3,p12||Middle Eocene|||||||
25940|Hampton Sandstone|43672|5|Briefly described|p330||Early Eocene|||||||
25940|Hampton Sandstone|43813|6|Mentioned|p133|||||||||
25940|Hampton Sandstone|43814|6|Mentioned|Fig.3,p115|||||||||
25940|Hampton Sandstone|43838|4|Described|p4||Tertiary|Interfingers with Pidinga Formation. Princess Royal Spongolite overlies. 35m thick.||||||12-JUL-16
25940|Hampton Sandstone|44133|4|Described|p181|Early Oligocene|Middle Eocene|Geological Province: Eucla Basin. Overlies the Pidinga Formation, Bring Member. Overlain by the Wilson Bluff Limestone. Thickness: 50m. ||||||
25940|Hampton Sandstone|44145|4|Described|p551 Tbl 4-27, p555-6, fig 4-194, p556|Middle Eocene|Middle Eocene|Eucla Basin. Max thickness > 85m. Varied fauna, commonly fragmented.||||Disconformably overlies Madura Formation. Overlain by / grades laterally into lower Wilson Bluff Limestone. Correlated with Pidinga Formation, Werillip Formation.|Limonite-stained sandstone, quartzose, variably calcareous and locally unlithified. Minor conglomerate.|
25940|Hampton Sandstone|44412|14|Not recorded|map legend||Eocene|M.-U.Eocene.||||||
25940|Hampton Sandstone|44695|5|Briefly described|Map Legend|Eocene|Eocene|(Middle-Late Eocene)||||||
25940|Hampton Sandstone|45149|4|Described|p62|||See also P60.||||||
25940|Hampton Sandstone|45168|6|Mentioned|p6|||See also Table 1||||||
25940|Hampton Sandstone|47054|6|Mentioned|p490|||||||||
25940|Hampton Sandstone|49060|6|Mentioned|Fig.5|||||||||
25940|Hampton Sandstone|60953|5|Briefly described|Map Legend|Eocene|Paleocene|Fluvial to esturine and marine sand and lignite. Geological Province: Eucla Basin.||||||27-APR-05
25940|Hampton Sandstone|61108|5|Briefly described|map legend|Eocene|Paleocene|Fluvial to estuarine and marine sand and lignite. Geological Province: Eucla Basin.||||||
25940|Hampton Sandstone|61155|5|Briefly described|p3, p17|Late Eocene|Middle Eocene|Interfingers with Pidinga Formation and Wilson Bluff Limestone, which also overlies this unit in part. Age: 45-36.5Ma. Max. thickness: 50m. Geological Province: Eucla Basin.||||||
25940|Hampton Sandstone|61197|5|Briefly described|p473, p475, p478 Fig.4, p481, p483, p488|Middle Eocene|Middle Eocene|Eucla Basin. Nearshore marine deposits. 0-30m thick. Has dendritic pattern in isopach maps. Probably extends into the Eucla Basin.|||||Medium-very coarse quartz sand; variably calcareous; weakly glauconitic; minor conglomerate.|
25940|Hampton Sandstone|61234|4|Described|p6, p7 Fig. 4|Eocene|Eocene|Overlain by Wilson Bluff Limestone. Geological Province: Eucla Basin. Calcareous, glauconitic and gritty shallow marine. Overlies  Pre-Tertiary rocks.||||||27-JUL-09
25940|Hampton Sandstone|61814|5|Briefly described|p22|Middle Eocene|Middle Eocene|Coarse and fine-grained lignitic and siliciclastic deposit, fluvial and estuarine.||||||08-FEB-10
25940|Hampton Sandstone|61856|5|Briefly described|p300 Fig.2, p304, p313-316  |Middle Eocene|Middle Eocene|Marine. The basal Tertiary unit in the central Eucla Basin.||||Is overlain conformably by Wilson Bluff Limestone.|Shallow marine sandstone, muddy at the base and glauconitic, calcareous and fossiliferous at top; grades upwards into neritic limestones.|22-JAN-15
25940|Hampton Sandstone|62369|5|Briefly described|p409, p410 Fig.4|Late Eocene|Middle Eocene|Estuarine-fluvial to marine deposits. Overlain by Wilson Bluff Limestone. Geological Province: Eucla Basin.||||||
25940|Hampton Sandstone|64340|6|Mentioned|p26 Tb. 5|Late Eocene|Late Eocene|Of Eundynie Group.||||||
25940|Hampton Sandstone|64646|6|Mentioned|p23 Fig. 3, p24 Fig. 4|Eocene||Geological Province: Eucla Basin.||||||08-FEB-10
25940|Hampton Sandstone|65194|5|Briefly described|p31, p136 Fig.4.37, p141, p164, p170|Late Eocene|Middle Eocene|Partially silicified fine- to medium-grained sand. Marine sediments in Gawler Craton and Lefroy Palaeovalley which interfinger with Pidinga Formation. High groundwater salinity. Correlated with the Wollubar Sandstone.||||||08-APR-16
25940|Hampton Sandstone|65260|6|Mentioned|p26-27, p27 Fig.20|Late Eocene||Of Eundynie Group. Interfingers with the Princess Royal Member in the Lefroy Palaeochannel. Fine-grained to gravelly glauconitic sand, locally weakly cemented to sandstone. Contains marine fauna, most commonly siliceous sponge spicules. Proposed by Clarke et al. (2003) to be subsumed into Pallinup Formation.||||||
25940|Hampton Sandstone|65891|6|Mentioned|p221 Fig.5. |Paleogene|Paleogene|East Eucla Basin. Lutetian age.||||||
25940|Hampton Sandstone|65942|2|Defined|p75|Middle Eocene|Middle Eocene|||Eucla Group||||28-MAY-10
25940|Hampton Sandstone|66131|6|Mentioned|p242 Fig.2|Eocene|Eocene|Middle-Late Eocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||||||
25940|Hampton Sandstone|67462|5|Briefly described|Map legend.|Eocene|Eocene|Bunda Plateau, Eucla Basin.||||||
25940|Hampton Sandstone|67921|5|Briefly described|Map legend|Eocene|Eocene|Occurs as a sheet beneath and between Ooldea, Barton and Paling Ranges.|||||Marine and non-marine quartz sand. Varicoloured, in part silicified and ferruginised.|
25940|Hampton Sandstone|68715|6|Mentioned|p30 Fig.5|Eocene|Eocene|Bunda Plateau, Eucla Basin. Middle Eocene age.||||||
25940|Hampton Sandstone|69598|5|Briefly described|p2, p9, p11 Tb.1, p29 Tb.4|Middle Eocene|Middle Eocene|Eucla Basin. Up to 85m thick. Potential carbon dioxide storage reservoir. Deposited in a shallow marine environment. ||Eundynie Group|||Spicular and calcareous sandstones.|
25940|Hampton Sandstone|69632|5|Briefly described|p26, p30|Eocene|Eocene|Eucla Basin.||||Overlies Madura Formation. Is overlain by Wilson's Bluff Formation.|A lenticular sandstone unit.|
25940|Hampton Sandstone|69648|4|Described|p4, p21-22, p25, p29, p36-37, map legend|Eocene|Eocene|Eucla Basin. Hampton Sandstone, Ooldea Sand, Yarle Sandstone are source of sand for Tertiary coastal sand units (including Wintrena Formation). Thickness: ~25-45m. No diagnostic fossils for age determination. Prospective for heavy mineral sand deposits. Low level mineralisation (best value was 8.37% heavy minerals in M169 28-30 m, EL 1654). Unclear in text: interbedded with/overlying? Wilson Bluff Limestone. Age: Middle to Late Eocene.||Burdunga Subgroup||With Ooldea Sand, overlies Pidinga Formation; conformably overlain by Paling Member (Wilson Bluff Limestone); unconformably overlain by Garford Formation.|Terrigenous clastic sediments; siliciclastic sands of marine and coastal origin; rare, minor clay horizons.|
25940|Hampton Sandstone|69649|5|Briefly described|p31, p32, p58|Eocene|Eocene|Eucla Basin. Represents a major marine transgression during Middle Eocene.|||||A sheet of very fine to coarse sand and grit, including heavy minerals, reworked by wave action into strandlines. Silcrete surface.|
25940|Hampton Sandstone|70397|5|Briefly described|p3|Middle Eocene|Middle Eocene|Eucla Basin.||Unit of Eucla Group.||Overlain by Wilson Bluff Limestone. Unconformably underlain by Madura Formation.||29-JUL-19
25940|Hampton Sandstone|70771|5|Briefly described|p27|||Eucla Basin.||||Unconformably overlies the Madura Formation.||
25940|Hampton Sandstone|70772|6|Mentioned|p2, p6-p7, p14, p22, p31, p38, p41|Eocene|Eocene|Bight Basin. Hosts possible microtektites.||||Unconformably overlies the Madura Formation.||
25940|Hampton Sandstone|70778|5|Briefly described|p4|||Intersected in Nundroo 3 DDH.|||||Clayey-sand.|
25940|Hampton Sandstone|71361|5|Briefly described|p5, p12|Middle Eocene|Middle Eocene|Eucla Basin. Interpreted to have been deposited when the Eucla Basin was flooded by the Southern Ocean.|c. 43 Ma|||Unconformably overlies the Madura Formation. Overlain by the Wilson Bluff Limestone.||
25940|Hampton Sandstone|71618|6|Mentioned|p124-125,127|Cenozoic|Cenozoic|Geological province: Eucla Basin.||||Disconformably overlies Madura Formation.||05-SEP-19
25940|Hampton Sandstone|71891|5|Briefly described|p6-p7|Cenozoic|Cenozoic|Eucla Basin, Coompana Province. 20-60m thick. Intepreted to have been deposited in marine, estuarine and fluvial environments.||||Overlies the Pidinga Formation. Overlain by the Wilsons Bluff Limestone.|Quartz-rich sandstone, carbonaceous sandstone.|12-MAY-23
25940|Hampton Sandstone|72344|5|Briefly described|p4|||Eucla Basin. Deposited as lenses and sheets in marine, estuarine and fluvial environments. See also p160.||||Overlies the Pidinga Formation. Overlain by the Wilson Bluff Limestone.|Poorly sorted limonite stained sandstone, typically quartz rich; includes subordinate gravel, conglomerate and siltstone.|
25940|Hampton Sandstone|72465|5|Briefly described|p9|Tertiary|Tertiary|Eucla Basin, Coompana Province. Deposited as lenses and sheets in marine, estuarine and fluvial environments.||||Overlies Pidinga Formation. Is overlain by Wilson Bluff Limestone.|Poorly-sorted limonite-stained sandstone, typically quartz-rich; includes subordinate gravel, conglomerate and siltstone.|
25940|Hampton Sandstone|72466|5|Briefly described|p9|Tertiary|Tertiary|Benbow et al. (1995). Eucla Basin, Coompana Province. Deposited as lenses and sheets in marine, estuarine and fluvial environments.||||Overlies Pidinga Formation. Is overlain by the Wilson Bluff Limestone.|Poorly-sorted limonite-stained sandstone, typically quartz-rich; includes subordinate gravel, conglomerate and siltstone.|
25940|Hampton Sandstone|72467|5|Briefly described|p9|Tertiary|Tertiary|Eucla Basin, Coompana Province. Deposited as lenses and sheets in marine, estuarine and fluvial environments.||||Overlies Pidinga Formation. Is overlain by Wilson Bluff Limestone.|Poorly-sorted limonite-stained sandstone, typically quartz-rich; includes subordinate gravel, conglomerate and siltstone.|
25940|Hampton Sandstone|72468|5|Briefly described|p9|||Eucla Basin. Deposited in marine, estuarine and fluvial environments.||||Underlain by Pidinga Formation. Overlain by Wilson Bluff Limestone.|Poorly sorted limonite-stained sandstone, typically quartz rich; includes subordinate gravel, conglomerate and siltstone.|
25940|Hampton Sandstone|72469|5|Briefly described|p9|||Eucla Basin. Deposited in marine, estuarine and fluvial environments.||||Underlain by Pidinga Formation. Overlain by Wilson Bluff Limestone.|Poorly sorted limonite-stained sandstone, typically quartz rich; includes subordinate gravel, conglomerate and siltstone.|
25940|Hampton Sandstone|72470|5|Briefly described|p9|||Eucla Basin. Deposited in marine, estuarine and fluvial environments.||||Underlain by Pidinga Formation. Overlain by Wilson Bluff Limestone.|Poorly sorted limonite-stained sandstone, typically quartz rich; includes subordinate gravel, conglomerate and siltstone.|
25940|Hampton Sandstone|72471|5|Briefly described|p9|||Eucla Basin. Deposited in marine, estuarine and fluvial environments.||||Underlain by Pidinga Formation. Overlain by Wilson Bluff Limestone.|Poorly sorted limonite-stained sandstone, typically quartz rich; includes subordinate gravel, conglomerate and siltstone.|
25940|Hampton Sandstone|72472|5|Briefly described|p9|||Eucla Basin. Deposited in marine, estuarine and fluvial environments.||||Underlain by Pidinga Formation. Overlain by Wilson Bluff Limestone.|Poorly sorted limonite-stained sandstone, typically quartz rich; includes subordinate gravel, conglomerate and siltstone.|
25940|Hampton Sandstone|73084|5|Briefly described|p16-17|Eocene|Eocene|Up to 20 m thick[?].||||Unconformably[?] underlain by Madura Formation. Overlain by Wilson Bluff Limestone.|Carbonaceous sandstone.|
25940|Hampton Sandstone|73111|5|Briefly described|Map legend.|Pleistocene|Eocene|Is overlain by un-named indurated, red-brown to orange calcareous aeolian sand.||||||
25940|Hampton Sandstone|73641|5|Briefly described|p5|Eocene|Eocene|Eucla Basin. <25m thick. Marine, estuarine and fluvial deposits.||||Overlies Pidinga Formation. Is overlain by Wilson Bluff Limestone.|Typically poorly sorted, limonite-stained, and quartz-rich sandstone; subordinate conglomerate and siltstone.|
81987|Hampton Ultramafic|72814|5|Briefly described|p201, Fig. 3, p202 Fig. 4, p204 Fig.6|||West of Zuleika Shear, Coolgardie Domain. [may be the same unit  as Hampton Hill Formation?]|||||Spinifex textured komatiitic [basalt] flows.|
81987|Hampton Ultramafic|73391|6|Mentioned|p103, 194, 244, 298, Appendices.|||Standing and Castleden (2002). Regional stratigraphic correlation chart of other workers. Coolgardie Domain, Kalgoorlie Terrane. Is offset 13 km in the Telegraph Syncline.||||Overlies Lindsays Basalt. Is overlain by Gleeson's Basalt.||
79014|Hangover Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2720 - 2680 Ma (inferred).|Marshall Pool Subgroup|||Sandstone, siltstone, felsic volcanic and volcaniclastic rock; metamorphosed. Mafic schist derived from basalt. Amygdaloidal basalt, aphyric basalt, basalt, komatiitic basalt; all metamorphosed.|
79014|Hangover Formation|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. |2726-2680 Ma (inferred)|Unit of Marshall Pool Subgroup.||Overlain by Mount Clifford Komatiite.|Sandstone and siltstone; metamorphosed, Felsic volcanic and volcaniclastic rock; metamorphosed; Mafic schist derived from basalt, basalt; amygaloidal, aphyric, metamorphosed; komatiitic basalt; relict pyroxene-spinifex texture; metamorphosed.|
79014|Hangover Formation|73596|6|Mentioned|p1159, 1162-1163|||Leonora eastern domain, Kalgoorlie Terrane. Described as ""affiliated"" with the Two Sisters Subgroup based on shared lithostatigraphic, geochemical and textural properties. Appears as Hangover Basalt, reflecting only the major component of the Formation.||Marshall Pool Subgroup.||Overlies Mount Leonora Formation. Is overlain by Mount Clifford Formation.|Basalts.|
77860|Hannans Subgroup|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2726 Ma (inferred) - 2680 Ma (inferred).|Kalgoorlie Group|Includes Paringa Basalt, Kapai Slate, Devon Consols Basalt, Kambalda Komatiite, Lunnon Basalt.|||
77860|Hannans Subgroup|71270|5|Briefly described|100k_interpgeop_lut.csv|||Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. ||Unit of Kalgoorlie Group.|Includes Devon Consols Basalt, Kambalda Komatiite, Kapai Slate, Lunnon Basalt, Paringa Basalt, Silver Lake Member.|||
77860|Hannans Subgroup|72095|4|Described|p4, p5, p6, 8|Neoarchean|Neoarchean|Eastern Goldfields, Yilgarn Craton. Geographically restricted to the Kalgoorie-Kambalda region.|2720-2690 Ma|Unit of Kalgoorlie Group|Includes Paringa Basalt, Kapai Slate, Devon Consols Basalt, Kambalda Komatiite and Lunnon Basalt.|Overlain unconformably or disconformably by Black Flag Group.||
77860|Hannans Subgroup|73596|6|Mentioned|p1162|||Kalgoorlie-Kambalda area, Kalgoorlie Terrane.|||Lunnon, Devon Consols, Paringa Basalts; Kambalda Komatiite; Kapai Slate.|Is overlain by Black Flag Group.||
41047|Hanns Camp Syenite|24196|6|Mentioned|p52|||See also Hanns Camp syenite.||||||
41047|Hanns Camp Syenite|64633|5|Briefly described|p7, p22, p58, p61 Fig.47, p62.|Neoarchean|Neoarchean||2664 +/- 2 Ma (Cassidy et al. 2002a).|||||
41047|Hanns Camp Syenite|73238|6|Mentioned|p15, p26|||Burtville Terrane.|2664 +/- 2 Ma.|||||10-JAN-23
75581|Hanns Jasper Formation|66113|5|Briefly described|Map legend|Archean|Archean|Burtville Terrane, Yilgarn Craton. Age c.2774 Ma. Dacitic volcaniclastic sandstone; crystal- and lithic-rich; metamorphosed.||||||
75581|Hanns Jasper Formation|68107|4|Described|p608 Fig.4, p609 Tb.1, p610-611, p616.|Neoarchean|Neoarchean|Irwin Hills-Stella Range Greenstone Belt, Burtville Terrane. Similar age to Palkapiti Formation.|2774 +/- 5 Ma (Wingate et al. 2010).||||Crystal- and lithic-rich, dacitic volcaniclastic sandstone.|22-SEP-14
75581|Hanns Jasper Formation|68186|5|Briefly described|Plate 1A|Archean|Archean|Burtville Terrane, Yilgarn Craton.|c.2774 Ma.||||Dacitic volcaniclastic sandstone, crystal- and lithic-rich; metamorphosed.|
75581|Hanns Jasper Formation|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Merolia Domain, Burtville Terrane, Eastern Goldfields Superterrane, Yilgarn Craton.  Felsic volcaniclastic sandstone dated. Pb/Pb SHRIMP magmatic crystallization age: 2774+/-5 Ma. See geochron file 193360.1.pdf, 193362.1.pdf (2010). |~2770 Ma|||Correlated with granite protoliths of Minigwal Suite.|Dacitic volcaniclastic sandstone; crystal and lithic rich; metamorphosed.|06-AUG-15
75581|Hanns Jasper Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|See also 100k_geologyp14_lut.csv and 500k_interpgeop14_lut.csv. Age derived from volcaniclastic sandstone sample (193362.1.pdf)|2774 Ma +/- 5 Ma (SHRIMP)||||Dacitic volcaniclastic sandstone; crystal and lithic rich; metamorphosed.|
75581|Hanns Jasper Formation|70802|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Burtville Terrane, Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events.|2774+\-5 Ma||||Dacitic volcaniclastic sandstone; crystal and lithic rich; metamorphosed|
75581|Hanns Jasper Formation|71168|6|Mentioned|p10|Neoarchean|Neoarchean|Burtville Terrane, Yilgarn Craton.|2774 +/- 5 Ma|||||
75581|Hanns Jasper Formation|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Burtville Terrane, Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma). Sample GSWA 193362 (volcaniclastic sandstone) yielded a weighted mean 207Pb/206Pb date of 2774+\-5 Ma, interpreted to be magmatic crystallisation age of the volcanic rock. See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 100k_geologyp14_lut.csv, 500k_interpgeop_lut.csv.|2774+\-5 Ma||||Dacitic volcaniclastic sandstone; crystal and lithic rich; metamorphosed|
75581|Hanns Jasper Formation|71493|5|Briefly described|p46|Neoarchean|Neoarchean|Burtville Terrane, Meriola Domain.|2774+/-5 Ma Pb/Pb||||Includes volcaniclastic sandstone.|
75581|Hanns Jasper Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||2774+/-5 Ma||||Dacitic volcaniclastic sandstone; crystal and lithic rich; metamorphosed.|
75581|Hanns Jasper Formation|73596|6|Mentioned|p1170|Neoarchean|Neoarchean|Irwin Hills Greenstone Belt, Burtville Terrane.|2774 +/- 5 Ma (MDA).|||||
41433|Hansens Folly Granite|24197|5|Briefly described|p26|Neoproterozoic|Neoproterozoic|Of O'Callaghan's Supersuite. I-type (granodioritic) ilmenite-bearing Mount Crofton type granite. Age: ~625Ma. Geological province: Paterson Province.||||||27-SEP-12
41433|Hansens Folly Granite|50436|5|Briefly described|p4.1|Neoproterozoic|Neoproterozoic|Geological Province: Paterson Orogen. Of the Mount Crofton Group (O'Callaghans Supersuite).|||||coarse-grained biotite syenogranite|27-SEP-12
31779|Harbutt Leucogranite|50436|5|Briefly described|p1.3, 3.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of the Krackatinny Supersuite. Age: 1310 +/- 4Ma (Shrimp).||||||
27163|Harms Sandstone|22754|5|Briefly described|p11 Tb. 3|Mesoproterozoic|Mesoproterozoic|Of the Glidden Group.||||||
27163|Harms Sandstone|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
27163|Harms Sandstone|32660|5|Briefly described|Table 6|||||||||
27163|Harms Sandstone|32728|5|Briefly described|Table 6|||||||||
27163|Harms Sandstone|36551|6|Mentioned|Table 10|||||||||
27163|Harms Sandstone|36885|4|Described|p180|||||||||
27163|Harms Sandstone|44155|5|Briefly described|p251 Tb.3-11|||60m thick.||Glidden Group||Overlies Crowhurst Group unconformably.|Quartz sandstone, interbedded shale and siltstone.|
27163|Harms Sandstone|44231|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Gliddens Group. Medium- and coarse-grained quartz sandstone, and purple shale and siltstone.||||||26-MAY-05
27163|Harms Sandstone|44397|14|Not recorded|p.15, Table3||Adelaidean|Glidden Group. Defn. on Tech.File E/52-9.||||||
27163|Harms Sandstone|44398|14|Not recorded|map legend||Adelaidean|||||||
27163|Harms Sandstone|45047|4|Described|p35|||Glidden Group.||||||
27163|Harms Sandstone|48927|2|Defined|p7|Adelaidean|Adelaidean|||||||
27163|Harms Sandstone|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Glidden Group.|||White pink and purple blocky thinly to thickly bedded fine medium and coarse grained quartz sandstone, purple laminated shale with rare green laminae, and minor thin interbeds of purple siltstone|
36822|Harts Range Metamorphic Complex|23858|5|Briefly described|p923|||||||||
36822|Harts Range Metamorphic Complex|61660|6|Mentioned|p2.|Proterozoic|Proterozoic|Irindina Province, eastern Arunta Region. ||||||
36822|Harts Range Metamorphic Complex|63562|6|Mentioned|p351|||Includes a small granitic body dated 387 +/- 4 Ma (Buick et al., 2001).||||||
36822|Harts Range Metamorphic Complex|64068|5|Briefly described|p25, 32, 199|Cambrian|Neoproterozoic|SHRIMP U-Pb dating of detrital zircons from southern Georgina Basin units has recently been undertaken, for comparison with metasedimentary units in the HRMC, as there are no available absolute age determinations (at the time of this study). Also Harts Range Complex p35.||||||
36822|Harts Range Metamorphic Complex|64571|6|Mentioned|p837|||||||||
36822|Harts Range Metamorphic Complex|66767|5|Briefly described|p59|Cambrian|Neoproterozoic|Irindina Province, Arunta Region. Crops out extensively in the Harts Range and extends as scattered low outcrops to the E and SE, into the Simpson Desert, and to the N near Mallee Bore. Similar zircon populations to similarly-aged sedimentary rocks in the adjacent Amadeus and Georgina Basins.|||||A thick metasedimentary succession with subordinate Paleozoic igneous units including mafic to ultramafic intrusions, metabasalts, granites and pegmatites.|
36822|Harts Range Metamorphic Complex|67479|6|Mentioned|p46|Ordovician|Cambrian|||||||
36822|Harts Range Metamorphic Complex|68316|5|Briefly described|pp777-782, pp784-786||Series 2|Inherited zircon in a granite intrusive into these rocks have yielded a SHRIMP U-TH-Pb age as young as c. 520 Ma (Buick et al. 2001).|< 520 Ma||Includes the Harts Range Meta-Igneous Complex.|Structurally underlain by the Entia Gneiss Complex.|Includes metasedimentary rocks.|
36822|Harts Range Metamorphic Complex|68697|5|Briefly described|v, p20, p22, p24, p46|Paleozoic|Neoproterozoic|Irindina Province, Arunta Region.|||Includes Brady and Irindina Gneisses.|||07-JAN-20
36822|Harts Range Metamorphic Complex|68997|4|Described|vii-viii,p55|Early Paleozoic|Neoproterozoic|Thickness 5-6km. Deposited in the Centralian Superbasin during the Neoproterozoic to earliest Palaeozoic prior to Ordovician mid-amphibolite to granulite facies metamorphism (Mawby 2000). The unnamed pelitic gneiss sampled from the Bungitina Metamorphics area (IC08JAW910) contained 445+\-7 Ma metamorphic zircon rims, indicating growth during early 450-300 Ma Alice Springs Orogeny (Scrimgeour and Raith 2001), which required thrusting of the Harts Range Metamorphic Complex over Palaeoproterozoic basement along the proximal Bruna Detachment Zone (eg Mawby et al 1999).|||Includes Yambla Gneiss.||Pelitic and semi-pelitic metasedimentary rocks, amphibolites and calc-silicates, with subordinate quartzite, marble and felsic gneiss.|
36822|Harts Range Metamorphic Complex|69031|5|Briefly described|p5|Cambrian|Neoproterozoic|Dominates the Irindina Province. Structurally interleaved with highly deformed granites.|||||Granulite-facies pelite, psammite, metamafic rocks, and calc-silicate rocks.|
36822|Harts Range Metamorphic Complex|69226|6|Mentioned|p238-239|||Eastern Arunta Inlier.||||||
36822|Harts Range Metamorphic Complex|69418|6|Mentioned|p3:31-32|||Irindina Province. Hosts mica deposits in the Harts Range/Plenty River fields. Source of abrasive quality garnets within alluvial sands in watercourses and sand dunes in the Harts Range area.||||||12-JUL-16
36822|Harts Range Metamorphic Complex|69427|5|Briefly described|p12:36-37|Cambrian|Neoproterozoic|Irindina Province. Separated from the structurally underlying Entia Gneiss Complex by the Bruna Granitic Gneiss.||||||12-JUL-16
36822|Harts Range Metamorphic Complex|69444|5|Briefly described|p29:1-10|Late Cambrian|Neoproterozoic|Formerly Harts Range Group (Joklik, 1955; Shaw et al., 1982). Irindina Province. Underwent upper amphibolite to granulite facies metamorphism during the Ordovician Larapinta Event.|||Irindina and Brady Gneisses.||An intensely deformed but flat-lying supracrustal succession consisting of pelitic and psammopelitic metasedimentary rocks, metabasite and calc-silicate rock, with subordinate marble, quartzite and felsic gneiss. Mid-amphibolite to granulite facies.|12-JUL-16
36822|Harts Range Metamorphic Complex|69458|6|Mentioned|p42:38|||Irindina Province. Garnetiferous metamorphic rocks are the source of abrasive-quality garnet in alluvial sands in the Harts Range area.||||||12-JUL-16
36822|Harts Range Metamorphic Complex|69510|6|Mentioned|p17|||480-460 Ma metamorphic ages for the Larapinta Event were obtained by Maidment (2005) and others.||||||
36822|Harts Range Metamorphic Complex|69917|5|Briefly described|p114, 138, 141,160,175,177-178|Paleozoic|Neoproterozoic|Cut by granite dykes: magmatism during the Alice Springs Orogeny was not continuous, but occurred in a series of discrete high-grade pulses, including at ca 382 and 360 Ma (Storkey 2004). See also p182, 184, 187, 189, 197, 198.|||Includes Brady, Yambla, Last Hope, Entire, Stanovos, Spriggs and ?Leprechaun Gneisses.|In contact with Paleoproterozoic Bruna Gneiss.||29-JUL-15
36822|Harts Range Metamorphic Complex|69932|6|Mentioned|p310-311|||Presented as Harts Range Metamorphic Igneous Complex on p310. May contain up to 80% Nd of an Archean component possibly from a sialic basement. Formed in association with 1780-1750 Ma back-arc opening.|||||Includes anorthositic gneisses.|
36822|Harts Range Metamorphic Complex|69937|6|Mentioned|p25, p28, p31|Paleozoic|Neoproterozoic||||Irindina Gneiss.|||
36822|Harts Range Metamorphic Complex|70825|6|Mentioned|p40, 42|||Arunta Region, North Australian Craton.||||||
36822|Harts Range Metamorphic Complex|71279|6|Mentioned|p353-354|||||||||
36822|Harts Range Metamorphic Complex|72375|5|Briefly described|p25,27|Paleozoic|Neoproterozoic|Geological province: Irindina Province.|||Includes Irindina Gneiss.|||
36822|Harts Range Metamorphic Complex|72515|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Jervois Range Special Map Sheet. Irindina Province.|||Includes the Yambla Gneiss.|||
36822|Harts Range Metamorphic Complex|72516|4|Described|iii, p7, p64, p78-79, p135-136|Cambrian|Neoproterozoic|Irindina Province. Formerly the Harts Range Group. Previously considered to include the Irindina Gneiss and the Brady Gneiss. |||Includes the Irindina Gneiss, Brady Gneiss, Yambla Gneiss, Pinnacle Gneiss, Last Hope Gneiss and the Leprechaun Gneiss.||Supracrustal succession of metamudstone, metagreywacke, metasandstone, metamafic igneous rocks and calc-silicate rocks with subordinate amounts of marble and felsic gneiss.|
36822|Harts Range Metamorphic Complex|72524|5|Briefly described|piii, p8, p13.|Cambrian|Neoproterozoic|Irindina Province. Deposited or emplaced during the Neoproterozoic-Cambrian and metamorphosed during the 480-460 Ma Larapinta Event. Includes migmatitc gneiss with maximum depositional age of 1019+/-23 Ma, and high grade metamorphism at 467+/-9 Ma. Source rock for Ghost gum granite.|||Yambla Gneiss, Stanovos Gneiss, Last Hope Gneiss, unnamed migmatitic gneiss.||Succession of metasedimentary rocks and subordinate igneous units [both piii and p8].|27-OCT-20
36822|Harts Range Metamorphic Complex|73184|6|Mentioned|p197|Ordovician|Ordovician|Peak metamorphism at ca 470 Ma in the Larapinta Event (Hand et al., 1999). [Possibly mentioned on p196 and 197 as Harts Range?] Cross-cut by numerous pegmatites with SHRIMP U-Pb monazite and zircon ages of ca 450-300 Ma.|ca 470 Ma|||||
39001|Harvey Formation|23880|5|Briefly described|p42|Eocene|Eocene|Geological Province: Yilgarn Craton.||||||
36843|Hatfield Formation|23727|4|Described|p9|||Underlying unit Maydon Basalt. Geological Province: Carlingup Terrane. Max. thickness: 1000 m.||||||
36843|Hatfield Formation|23728|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Annabelle Volcanics. Underlying unit Maydon Basalt. Geological Province: Yilgarn Craton.||||||07-NOV-08
36843|Hatfield Formation|23752|4|Described|p6|Archean|Archean|Geological Province: Carlingup Terrane.||||||07-NOV-08
36843|Hatfield Formation|23754|5|Briefly described|Map Legend|Archean|Archean|Underlying unit Maydon Basalt. Geological Province: Yilgarn Craton.||||||07-NOV-08
36843|Hatfield Formation|64580|4|Described|map legend|Neoarchean|Mesoarchean|Metasedimentary clastic rocks, minor dacitic volcanic and volcaniclastic rocks.||||||15-DEC-08
36843|Hatfield Formation|65487|6|Mentioned|p6|||Uppermost unit in the Carlingup Greenstone Belt; consists of fine-grained clastic metasediments, minor dacitic metamorphosed volcanic and volcaniclastic rocks, and minor coarse-grained metaclastic rocks interbedded with pelitic rocks; at least 1 km thick.||||||
36843|Hatfield Formation|68108|5|Briefly described|p651 Tb.4|Mesoarchean|Mesoarchean|Southern Cross Domain. Age of rhyolite; stratigraphic relationship uncertain. U-Pb geochronology by Nelson (1995).|2958 +/- 4 Ma||||Rhyolite.|08-OCT-14
36843|Hatfield Formation|69404|5|Briefly described|p10, p10 Fig.11|||Carlingup Terrane.||||Overlies the Maydon Basalt.|Felsic to intermediate volcanic rocks, sandstone, siltstone, shale and wacke.|
36843|Hatfield Formation|69617|5|Briefly described|p155|||||||Overlies Maydon Basalt.|Includes felsic volcanic and sedimentary rocks.|
36843|Hatfield Formation|70802|5|Briefly described|500k_interpgeop14_lut.csv|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Youanmi Terrane events.|3200-2958 Ma (inferred)||||Metasedimentary clastic rocks; minor dacitic volcanic and volcaniclastic rocks|
36843|Hatfield Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Youanmi Terrane.|||||Metasedimentary clastic rocks; minor dacitic volcanic and volcaniclastic rocks.|
31475|Hawley Member|12758|5|Briefly described|p21, P10 Fig. 10|Early Cretaceous|Early Cretaceous|Of the Carnac Formation. Overlain by Charlotte Sandstone. Directly overlain by South Perth Shale (in Marri 1 drillhole). Max. thickness: 666m in type section. Geological Province: Vlaming Sub-basin.||||||27-JUL-09
31475|Hawley Member|14227|5|Briefly described|Enclos. 2|Berriasian|Berriasian|Of Carnac Formation (Parmelia Group). Overlies Mangles Member. Presented as Hawley.||||||07-FEB-11
31475|Hawley Member|24443|5|Briefly described|Fig.31|Early Cretaceous|Late Jurassic|Of Carnac Formation. Conformably overlies Mangles Member. Conformably overlain by Charlotte Sandstone. Geological Province: Perth Basin.||||||
31475|Hawley Member|50108|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Carnac Formation (Parmelia Group). Geological Province: Perth Basin.||||||27-JUL-09
31475|Hawley Member|69182|6|Mentioned|Ch2 p15|Lower Cretaceous|Lower Cretaceous|Perth Basin. ||Carnac Formation||||
31475|Hawley Member|71958|6|Mentioned|p45-p46|||Vlaming Sub-basin.||Carnac Formation||Unconformably overlain by the Charlotte Supersqeuence.||
23645|Haycock Marl|6876|6|Mentioned|p100 Fig.5.|Cretaceous|Cretaceous|||||||
23645|Haycock Marl|14228|5|Briefly described|p5 Fig.2, p9, p16|Turonian|Turonian|||||Overlies Winning Group.|Marine carbonaceous clay with bioturbated calcilutite.|
23645|Haycock Marl|23433|5|Briefly described|p111|Cretaceous|Cretaceous|||||||
23645|Haycock Marl|23726|5|Briefly described|p8 Fig 2c|Late Cretaceous|Early Cretaceous|Overlying unit Toolonga Calcilutite. Underlying unit Windalia Radiolarite. Geological Province: Carnarvon Basin.||||||
23645|Haycock Marl|24160|5|Briefly described|p36, 38|Cretaceous|Cretaceous|Dampier Sub-basin.||Winning Group||Overlies Windalia Radiolarite conformably. More calcareous lateral equivalent of Gearle Siltstone. Is conformably overlain by Toolonga Calcilutite.|Two units of argillaceous calcilutite and marl, separated by a thin, laterally persistent claystone horizon.|
23645|Haycock Marl|24351|5|Briefly described|Plate 4 (in pocket)|Late Cretaceous|Early Cretaceous|Geological Province: Exmouth Plateau.||||||13-DEC-07
23645|Haycock Marl|40617|6|Mentioned|p15|||||||||
23645|Haycock Marl|40800|2|Defined|p4|early Albian|early Albian|||||||
23645|Haycock Marl|41271|3|Fully described|p152|||||||||
23645|Haycock Marl|41436|6|Mentioned|p48|||||||||
23645|Haycock Marl|41438|6|Mentioned|p109|||||||||
23645|Haycock Marl|41439|5|Briefly described|p123|||||||||
23645|Haycock Marl|41732|6|Mentioned|Fig.3|||||||||
23645|Haycock Marl|42116|5|Briefly described|Fig.1 P6|||||||||
23645|Haycock Marl|42598|6|Mentioned|Fig 5(P 14)|||||||||
23645|Haycock Marl|43712|5|Briefly described|p11||Aptian|||||||
23645|Haycock Marl|43722|6|Mentioned|p10-11|||||||||
23645|Haycock Marl|43724|5|Briefly described|p29|||||||||
23645|Haycock Marl|43826|6|Mentioned|Fig.2,p163|Late Cretaceous|Early Cretaceous|||||||01-MAR-10
23645|Haycock Marl|43827|5|Briefly described|p193|Turonian|Albian|Found at ODP sites 762,763||||||
23645|Haycock Marl|49942|4|Described|p4 Fig.3, p11|Late Cretaceous|Late Cretaceous|Unconformably overlies Gearle Siltstone. Unconformably overlain by Toolonga Calcilutite. Mudstone to marl. Max. thickness: 302 m. Deposited in a low energy inner- to middle-shelf environment. Geological Province: Gascoyne Platform.||||||
23645|Haycock Marl|60384|5|Briefly described|p244, p243 Fig 2a, p259|Coniacian|Turonian|Perth and Southern Carnarvon Basins.||||Overlies Winning Group in places. Overlain by Toolonga Calcilutite.|Transitional mudstone to marl|
23645|Haycock Marl|61811|5|Briefly described|p3 Fig.2, p8, p9 Table 3, p17.|Turonian|Turonian|Northern Perth Basin.||||Overlies Gearle Siltstone. Is overlain by Toolonga Calcilutite.|Friable pink bioturbated marl with Chondrites burrows; glauconitic sand and fish debris thicker near base; rare Planolites burrows and chalk infillings towards top.|
23645|Haycock Marl|62734|5|Briefly described|p1362 Fig. 2|Late Cretaceous|Early Cretaceous|Geological Province: Barrow Sub-basin.||||||01-SEP-08
23645|Haycock Marl|62837|5|Briefly described|Stratigraphic columns|Early Cretaceous|Early Cretaceous|Age: ~114-90Ma. Geological Province: Exmouth Plateau, Rankin Platform and Beagle Sub-basin||||||01-MAR-10
23645|Haycock Marl|63068|5|Briefly described|p44 Fig. 2|Turonian|Turonian|Of the Winning Group. Thin unit that overlies Gearle Siltstone, but which is often included as part of upper Gearle Siltstone. Geological Province: Carnarvon Basin.||||||27-FEB-07
23645|Haycock Marl|64580|6|Mentioned|map legend|||Of Winning Group.||||||15-DEC-08
23645|Haycock Marl|64635|5|Briefly described|p4 Fig.3, p7  |Turonian|Cenomanian|||||||
23645|Haycock Marl|66126|6|Mentioned|p206|Early Cretaceous|Early Cretaceous|Carnarvon Basin.||||||
23645|Haycock Marl|67200|5|Briefly described|p8 fig 6, |Cretaceous|Cretaceous|||||Overlies Windalia Radiolarite, unconformably overlain by Toolonga Calcilutite|Crudely bedded marl.|
23645|Haycock Marl|67340|6|Mentioned|p6|Late Cretaceous|Late Cretaceous|Northern Perth Basin.||||||
23645|Haycock Marl|67368|6|Mentioned|p209 Fig.4.|Late Cretaceous|Albian|||||Overlies Windalia Radiolarite. Is overlain by Toolonga Calcilutite.||
23645|Haycock Marl|67784|6|Mentioned|p30 Fig.7||Cenomanian|Carnarvon Basin.||||||
23645|Haycock Marl|68206|6|Mentioned|p30|||Carnarvon Basin.||||||
23645|Haycock Marl|69166|6|Mentioned|500k_geologyp08_lut.csv|Cretaceous|Cretaceous|||Winning Group||||
23645|Haycock Marl|69182|6|Mentioned|Ch3 p12|Turonian|Turonian|Carnarvon Basin. ||||||
23645|Haycock Marl|69185|5|Briefly described|500k_geologyp08_lut.csv|Cretaceous|Cretaceous|Of Northern Carnarvon Basin. Comprises northern part of the Winning Group.||Unit of Winning Group.||||
23645|Haycock Marl|69297|5|Briefly described|p249|Santonian|Turonian|Gascoyne Sub-basin of the Southern Carnarvon Basin. ||||Unconformably overlies the Gearle Siltstone. Overlain by the Toolonga Calcilutite.|Marl.|
23645|Haycock Marl|69689|6|Mentioned|p16|Cretaceous|Cretaceous|Northern Carnarvon Basin.||||Overlies Muderong Shale.||
23645|Haycock Marl|70066|5|Briefly described|Dampier: Fig.2. Exmouth: Fig.2|Coniacian|Albian|See also Regional: Fig.6. Northern Carnarvon Basin.||Winning Group.||Overlies and is intercalated with Gearly Siltstone. Is overlain by Toolonga Calcilutite.||
75578|Hazlett beds|65074|4|Described|p351 fig 4-37, p351, p356 Tb. 4-12, p360|Mesozoic|Mesozoic|See also p361 Tb. 4-14, p362. Of SW Birrindudu Basin. Non-fossiliferous; possibly Triassic. Forms cappings on mesas and plateaus.||||Overlies Redcliff Pound Group (unconformably). Equivalent to Larranganni beds.|Quartz sandstone, siltstone, white claystone.|
75578|Hazlett beds|70826|6|Mentioned|p7 tbl 4|Mesozoic|Mesozoic|Eastern Canning Basin.||||||
75578|Hazlett beds|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone, claystone|
68510|Hearson Cove Monzogranite|63441|2|Defined|p10 Tb. 2, p37|Archean|Archean|Of Maitland River Supersuite. Forms northern part of Dampier Granitic Complex. Unconformably overlain by parts of Fortescue Group. Geological province: Pilbara Craton. Distinctive foliated porphyritic monzogranite. Intruded by 2725Ma Gidley Granophyre.||||||07-FEB-11
68510|Hearson Cove Monzogranite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Maitland River Supersuite. Geological province: Pilbara Craton.  Monzogranite and syenogranite containing microcline megacrysts; metamorphosed.||||||07-NOV-08
68510|Hearson Cove Monzogranite|64580|4|Described|map legend||Mesoarchean|Of Maitland River Supersuite. Monzogranite and syenogranite containing microcline megacrysts; metamorphosed.||||||15-DEC-08
68510|Hearson Cove Monzogranite|67201|4|Described|p16-17 Fig.9|Archean|Archean|Pilbara Craton. In Roebourne-Karratha area.||Maitland River Supersuite|||Monzogranite and syenogranite containg microcline megacrysts; metamorphosed.|
68510|Hearson Cove Monzogranite|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Maitland River Supersuite.|||Monzogranite and syenogranite containing microcline megacrysts; metamorphosed|
68510|Hearson Cove Monzogranite|70775|5|Briefly described|p15, p53|Mesoarchean|Mesoarchean|Pilbara Craton. Together with the Miaree Granite and the Erramurra Monzogranite forms the Dampier Granitic Complex. This unit is intermittently exposed across an area of 600km ^2 on the Burrup Peninsula and the Dampier Archipelago.|2999 +/- 10 Ma (Wingate and Hickman, 2009a)|Maitland River Supersuite|||Monzogranite and syenogranite containing microcline megacrysts; metamorphosed.|
68510|Hearson Cove Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, syenogranite|
68510|Hearson Cove Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|De Grey Superbasin.|2999+/-10 Ma.|Maitland River Supersuite|||Monzogranite and syenogranite containing microcline megacrysts; metamorphosed.|
80966|Heavitree Formation and Bitter Springs Group|72034|5|Briefly described|500k_interpgeop16_lut|Tonian|Tonian|Amadeus Basin (Phase 1). Shown informally grouped with Bitter Springs Group. See also superseded name Heavitree Quartzite.|||||Quartz sandstone, sandstone and conglomerate, dolomite, stromatolitic dolomite and siltstone.|
30235|Heines Member|12099|6|Mentioned|p683|Orosirian|Orosirian|||Unit in Wilthorpe Formation.||||04-MAR-13
30235|Heines Member|22694|6|Mentioned|p7|||Wilthorpe Formation||||||
30235|Heines Member|22940|4|Described|Fig.6 p14, Tb2 p12|Paleoproterozoic|Paleoproterozoic|of Wilthorpe Formation, Padbury Group.||||||07-NOV-08
30235|Heines Member|23744|5|Briefly described|p10 Table 1|Paleoproterozoic|Paleoproterozoic|Of Wilthorpe Formation. Geological Province: Padbury Basin.||||||07-NOV-08
30235|Heines Member|23747|4|Described|p15|Paleoproterozoic|Paleoproterozoic|Previously mapped as Wilthorpe Conglomerate. Of Wilthorpe Formation. Geological Province: Padbury Basin.||||||07-NOV-08
30235|Heines Member|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Wilthorpe Formation. Geological Province: Padbury Basin.||||||
30235|Heines Member|23749|4|Described|p13|Proterozoic|Proterozoic|Of Wilthorpe Formation. Geological Province: Padbury Basin.||||||
30235|Heines Member|23750|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Wilthorpe Formation. Geological Province: Padbury Basin.||||||
30235|Heines Member|49896|5|Briefly described|p57 App. 4|||Of the Wilthorpe Formation. Polymictic conglomerates (Pirajno 1997). See also Heins Member.||||||25-SEP-12
30235|Heines Member|50222|5|Briefly described|p320 Fig. 3, p327|Paleoproterozoic|Paleoproterozoic|Of the Wilthorpe Formation (Padbury Group).  Contains polymictic conglomerate, sandstone and shale.   Geological Province: Padbury Basin.||||||07-NOV-08
30235|Heines Member|62289|5|Briefly described|plate 1|Palaeoproterozoic|Palaeoproterozoic|Of Wilthorpe Formation (Padbury Group). Quartz wacke, siltstone, and shale; minor polymictic conglomerate. Geol. Prov: Padbury Basin.||||||
30235|Heines Member|64580|4|Described|map legend||Paleoproterozoic|Of Wilthorpe Formation. Quartz wacke; siltstone; and shale; minor polymicitic conglomerate.||||||15-DEC-08
30235|Heines Member|65408|5|Briefly described|p83.|Paleoproterozoic|Paleoproterozoic|||Unit in Wilthorpe Formation.|||Polymictic conglomerate.|14-SEP-12
30235|Heines Member|65411|5|Briefly described|p88.|Paleoproterozoic|Paleoproterozoic|Local equivalent of Beatty Park Member.||Unit in Wilthorpe Formation.||Base is in faulted contact with Narracoota Formation. Is conformably overlain by Robinson Range Formation.|Polymictic conglomerate, quartz sandstone and shale.|
30235|Heines Member|65419|2|Defined|p38, pp42-44.|Paleoproterozoic|Paleoproterozoic|Defined in this study. Corresponds to that part of the Wilthorpe Conglomerate of Gee (1979), Windh (1992) and Martin (1994 in prep.) that outcrops on central Bryah 1:100 000 sheet. Lateral equivalent of the Beatty Park Member. Named after the Heines Find prospect. No type section nominated; type area is c.5 km NE of Murphy Well. Thickness c.1000 m. Basal conglomerate contains no volcanic clasts from the underlying Narracoota Formation.||Unit in Wilthorpe Formation.||Is faulted against the Narracoota Formation. Is inferred to be conformably overlain by Robinson Range Formation.|Upward-fining succession of polymictic conglomerate with a carbonate matrix, lithic wacke, sandstone, quartz-hematite schist and quartz-sericite-hematite schist.|
30235|Heines Member|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic|||Wilthorpe Formation|||Quartz wacke; siltstone; and shale; minor polymicitic conglomerate|
30235|Heines Member|69003|5|Briefly described|p16|||Padbury Basin.||Wilthorpe Formation.||Locally overlies Labouchere Formation.|Turbidites.|
30235|Heines Member|69166|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|||Wilthorpe Formation|||Quartz wacke; siltstone; and shale; minor polymicitic conglomerate.|
30235|Heines Member|69596|5|Briefly described|p10|||Padbury Basin.||Wilthorpe Formation.||||
30235|Heines Member|70804|5|Briefly described|p2-p3, p19-p20, p43, plate 1||Orosirian|The type area is located near Durack Well on BRYAH where this unit is folded in a syncline. Includes rocks previously mapped as the Wilthorpe Conglomerate by Gee (1987). Approximately 600m thick. |c. <2000 Ma|Wilthorpe Formation||Overlies (tectonically) the Narracoota Formation. Conformably overlain by the Robinson Range Formation.|Polymictic conglomerate, sandstone, shale.|27-FEB-23
30235|Heines Member|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate|
30235|Heines Member|71269|4|Described|1m_geologyp12_lut.csv|||Of Padbury Basin. Events: Capricorn Orogeny (1817-1772 Ma).||Unit of Wilthorpe Formation.|||Upward-fining succession of polymictic conglomerate with a carbonate matrix, lithic wacke, sandstone, quartz-hematite schist and quartz-sericite-hematite schist.|
79291|Hercules Gneiss|70089|5|Briefly described|p261, 263, 265-279|Archean|Archean|Tropicana Zone, Albany-Fraser Orogen. Hosts disseminated and vein-related Au. Mineralisation occurred at c.2100 Ma.  Zircon U-Pb, epsilon Hf ages tabulated and discussed in detail, as is its (sanukitoid) geochemistry.|2692 +/- 16 Ma.||||Mafic (gabbroic), dioritic to quartz-monzodioritic gneisses with well-defined, layered gneissic fabric, locally with blue quartz. Alteration (red-stained feldspars) overprint. Early and prolonged granulite-facies conditions.|
79291|Hercules Gneiss|70182|5|Briefly described|p4, p14|Neoarchean|Neoarchean|Tropicana Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen.|2692 +/- 16 Ma (magmatic crystallisation)||||Includes hydrothermally altered sanukitoids.|
79291|Hercules Gneiss|70256|5|Briefly described|p4-6, p10, p13, p15, p19-29|Archean|Archean|New name. Amphibolite- to granulite-facies basement rocks of the Tropicana Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen. Associated with the Hercules, Atlantis and Neale gold prospects. Geochronology determinations (zircon U-Pb, Re-Os) tabulated: 2826 +/- 166 Ma to 2644 Ma (protoliths); results discussed in detail. Major and trace element diagrams; geochemistry discussed. Gold mineralisation discussed.|2692 +/- 16 Ma.||||Felsic to intermediate granitic gneiss locally interlayered with mafic (gabbroic) gneiss; typically with well-defined layered gneissic fabric; sanukitoids. Overprinted by mylonitic fabric. Sulfide-bearing quartz veins and calcite veins.|
79291|Hercules Gneiss|70802|4|Described|250k_pre_mesozoic_interpgeop_lut.csv|Paleoproterozoic|Neoarchean|Geological province: Tropicana Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage II (1225-1140 Ma); Albany-Fraser Orogeny (1330-1140 Ma); Albany-Fraser Orogeny Stage I (1330-1260 Ma); Biranup Orogeny (1710-1620 Ma); Ngadju Event (1780-1760 Ma); Salmon Gums Event (1815-1800 Ma); Tropicana Event (2520-2505 Ma); Atlantis Event (2720-2550 Ma). Sample GSWA 192523 (amphibolitic gneiss) yielded a weighted mean 207Pb*/206Pb* date of 2692+\-16 Ma, interpreted as magmatic crystallization age of the igneous protolith of the gneiss. Sample GSWA 192524 (quartzofledpsathic gneiss) yielded 207Pb*/206Pb* dates of 2677-2603 Ma, interpreted to indicate the timing of granulite-facies metamorphism. Sample GSWA 192531 (metagranite) yielded  207Pb*/206Pb* dates of 2683-2585 Ma, interpreted to indicate the timing of zircon growth under granulite-grade conditions. Sample GSWA 192532 (granitic gneiss) yielded  a 207Pb*/206Pb* date of 2826+\-83 Ma, interpreted as magmatic crystallisation age of the igneous protolith, and 207Pb*/206Pb* dates of 2718-2580 Ma, interpreted as timing of zircon growth under granulite-grade conditions. Sample GSWA 192552 (monzodioritic gneiss) yield a concordia age of 2726+\-14 Ma, interpreted as magmatic crystallisation age of the igneous protolith. See also geochron files.|2795+\-12 Ma; 1783+\-3 Ma|Unit of Neale Supersuite.|||Metadiorite and quartz metamonzodiorite gneiss; locally intruded by Paleoproterozoic granite and mafic rocks|
79291|Hercules Gneiss|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Neoarchean|Tropicana Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen.|Max age 2795+/-12 Ma, min age 1783+/-3 Ma.|Neale Supersuite||Remnants included in McKay Creek Metasyenogranite, Bobbie Point Metasyenogranite.|Metadiorite and quartz metamonzodiorite gneiss; locally intruded by Paleoproterozoic granite and mafic rocks.|
28604|Hester granite|39161|6|Mentioned|p49|||||||||
26612|Hibberson Dolomite|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26612|Hibberson Dolomite|32660|5|Briefly described|Table 3|||||||||
26612|Hibberson Dolomite|32728|5|Briefly described|p33|||||||||
26612|Hibberson Dolomite|36551|6|Mentioned|Table 10|||||||||
26612|Hibberson Dolomite|36885|4|Described|p184|||||||||
26612|Hibberson Dolomite|38988|6|Mentioned|Fig.4|||||||||
26612|Hibberson Dolomite|44140|5|Briefly described|p294 Tb.4-1|Paleoproterozoic|Paleoproterozoic|25 m thick.||Crowhurst Group||Conformably overlies Collett Siltstone.|Pink or yellow dolomite, oolitic dolomite and dolomite breccia; stromatolites common.|07-MAR-18
26612|Hibberson Dolomite|44231|5|Briefly described|Map Legend||Mesoproterozoic|Of the Crowhurst Group.  Massive dolomite, may be stromatolitic; minor sandy oolitic dolomite breccia, and dolomitic sandstone. Age: c.1500Ma? Geological Province: Crowhurst Basin.||||||26-MAY-05
26612|Hibberson Dolomite|44397|14|Not recorded|p.9,17, Table 2||Carpentarian|Crowhurst Group. Defn. on Tech.File E/52-9.||||||
26612|Hibberson Dolomite|44398|14|Not recorded|map legend||Carpentarian|||||||
26612|Hibberson Dolomite|45047|5|Briefly described|p28|||Crowhurst Group.||||||
26612|Hibberson Dolomite|64104|6|Mentioned|p76 fig 10|Paleoproterozoic|Paleoproterozoic|||Unit in Crowhurst Group.||||
26612|Hibberson Dolomite|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Pink to yellow massive, thinly bedded to laminated and possibly stromatolitic dolomite, minor interbeds of sandy oolitic dolomite breccia and fine dolomitic sandstone|
27432|Hibernia Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p228|Eocene|Eocene|Pattillo and Nicholls (1990). In figure, Fm = Formation. Geological Province: Bonaparte Basin.||||||01-MAR-10
27432|Hibernia Formation|13194|4|Described|p383 Tb. 4-16, p396 fig 4-60|Cenozoic|Cenozoic|Up to 1300m thick. Thickest in Vulcan Graben and Ashmore Platform.||||Overlain by Cartier Formation (disconformably). Overlies Bathurst Island Group.|Limestone, sandstone; minor shale and marl.|
27432|Hibernia Formation|13224|6|Mentioned|p485 fig 3|Oligocene|Paleocene|||||||
27432|Hibernia Formation|22663|5|Briefly described|AC97 1-4 Fig.4||Eocene|Of the Woodbine Group.||||||26-SEP-06
27432|Hibernia Formation|23377|6|Mentioned|p212 Fig.5||Eocene|Of Vulcan Sub-basin.||||||26-SEP-06
27432|Hibernia Formation|24171|5|Briefly described|p722 Fig. 3|Tertiary|Tertiary|Geological Province : Vulcan Sub-Basin||||||01-MAR-10
27432|Hibernia Formation|24218|5|Briefly described|p850|Eocene|Eocene|Geological Province: Bonaparte Basin.||||||
27432|Hibernia Formation|41437|6|Mentioned|Fig.3|||||||||
27432|Hibernia Formation|41532|4|Described|p308|||Mention Fig.15.||||||26-SEP-06
27432|Hibernia Formation|41690|6|Mentioned|p6|||||||||
27432|Hibernia Formation|41733|6|Mentioned|Fig.3|||||||||
27432|Hibernia Formation|42034|4|Described|Fig.4 P11|||||||||
27432|Hibernia Formation|42053|5|Briefly described|Fig.2 P29|||||||||01-MAR-10
27432|Hibernia Formation|42057|6|Mentioned|Fig.3 P70|||||||||
27432|Hibernia Formation|42066|5|Briefly described|Fig.3 P199|||||||||01-MAR-10
27432|Hibernia Formation|42081|5|Briefly described|Fig.2 P291|||||||||
27432|Hibernia Formation|42151|6|Mentioned|Fig.3 P57|||||||||
27432|Hibernia Formation|42442|3|Fully described|p30|Eocene|Paleocene|||||||
27432|Hibernia Formation|43699|6|Mentioned|Fig.6,p10|Eocene|Paleocene|||||||
27432|Hibernia Formation|43707|5|Briefly described|Fig.3,p4-5||Tertiary|||||||
27432|Hibernia Formation|43739|6|Mentioned|Fig.5,p38|Oligocene|Paleocene|||||||
27432|Hibernia Formation|49637|5|Briefly described|Fig. 3|Eocene|Paleocene|Includes the Grebe Sandstone Member. Geological Province: Vulcan Sub-basin.||||||07-FEB-11
27432|Hibernia Formation|60634|6|Mentioned|p1168 Fig.3. |Eocene|Eocene|||Unit in Woodbine Group.||Overlies Grebe Formation. Is overlain by Prion Formation.||
27432|Hibernia Formation|61155|5|Briefly described|p15, p16|Early Oligocene||See also Hibernia Formation. Age: >32.5Ma. Max. thickness: 1200m in Sahul Platform region. Geological Province: Bonaparte Basin / Ashmore and Sahul Platforms, Vulcan and Petrel Sub-basins; and Money Shoal Basin - north. ||||||
27432|Hibernia Formation|61548|6|Mentioned|p480 Fig.3|Eocene|Eocene|Northern Bonaparte Basin.||||||
27432|Hibernia Formation|61550|6|Mentioned|p495 Fig.2. |Eocene|Eocene|||Unit in Woodbine Group.||Overlies Grebe Formation. Is overlain by Prion Formation.||
27432|Hibernia Formation|62837|5|Briefly described|Stratigraphic columns|Eocene|Eocene|Age: ~50-~42Ma. Geological Province: Western Bonaparte Basin and Northern Bonaparte Basin.||||||22-JAN-07
27432|Hibernia Formation|64695|5|Briefly described|p260, p261 Fig.6, p262 Fig.8|Eocene|Eocene|Northern Bonaparte Basin.||||Overlies Grebe Formation. Is overlain by Prion Formation, and unconformably by Oliver Formation.||
27432|Hibernia Formation|64697|5|Briefly described|p84 Fig.2 |Eocene|Eocene|||||||
27432|Hibernia Formation|65680|6|Mentioned|p709 Fig.2.|Priabonian|Lutetian||||Includes Grebe Sandstone Member.|Overlies Johnson Formation. Is unconformably overlain by Cartier Formation and Oliver Sandstone Member.||
27432|Hibernia Formation|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Eocene|Paleocene|Unit in the Woodbine Group. Underlies the Prion Formation, overlies the Grebe Formation. Mount Ashmore Dome. Limestone dominated with claystone at the base.||||||
27432|Hibernia Formation|68223|6|Mentioned|p178 Fig.3, p179 Fig.4|Eocene|Eocene|||||||
27432|Hibernia Formation|69452|5|Briefly described|p36:15, 22|Paleogene|Paleogene|Bonaparte Basin.||Woodbine Group.|Grebe Sandstone Member.|||12-JUL-16
27432|Hibernia Formation|69673|6|Mentioned|p174|||||||||
27432|Hibernia Formation|70061|5|Briefly described|Regional geology Figs.6-7, p12|Eocene|Eocene|See also Sahul: Fig.2. Vulcan: Fig.2.||Woodbine Group.|Grebe Sandstone Member.|Overlies Johnson Formation. Is overlain by Prion Formation.||12-JUL-16
41911|Hickey Ricken Granite|70156|4|Described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma).|2654-2600 Ma (inferred)||||Granite, undivided|
41911|Hickey Ricken Granite|70794|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton. Also 2_5m_interpgeop15_lut.csv.|2654-2600 Ma inferred||||Granite, undivided.|
41911|Hickey Ricken Granite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||||||Granite, undivided.|
77936|Hickies Bore Basalt|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||2820 - 2711 Ma (inferred).||||Fine-grained mafic schist; locally hornfelsed, amphibolitized or epidotized. Basalt; fine grained with local pyroxene-spinifex texture; includes medium-grained layers and lenses; minor interflow sedimentary rocks; metamorphosed.|
77936|Hickies Bore Basalt|70326|3|Fully described|p336,338-9,341,343,346-8,351,353-4,360-4|Neoarchean|Neoarchean|Geological province: Agnew region, Ora Banda Domain, Kalgoorlie Terrane, Yilgarn Craton. Subaqueous extrusions and comagmatic intrusions of high-Mg tholeiitic composition that are slightly enriched in REEs. The sequence becomes progressively more fractionated with time. Thickness: 525 m thick (upper HBB = 85 m; lower HBB = 350 m, intrusions = 5-100 m). Top and bottom observed in several drillholes on the Western limb, and the HBB is observed sporodically in outcrop. Intruded by several mafic sills (one 40-50 m thick,and at least three others that are 3-5 m thick) in the lower section. Major and trace element geochemical analysis on Table 4 p342-346.||||Overlain by Songvang Basalt. Underlain by Donegal Komatiite. Correlable to Wongi, Burbank and McFarlanes basalts.|Upper HBB: massive basalt. Lower HBB: massive and pillow basalt (amygdaloidal in places). Includes sulphidic mudstone, dolerite and gabbro, ultrabasic cumulate, basalt. Submarine pillow, sheet flows, differentiated comagmatic intrusions.|29-JUL-19
77936|Hickies Bore Basalt|71212|5|Briefly described|intro p2, intro p3|||Yilgarn Craton. ||||Overlies the Donegal Komatiite. Interbedded with (and overlain by) the Satellite Igneous Complex.||
77936|Hickies Bore Basalt|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2820-2711 Ma (inferred)||||Basalt; fine grained with local pyroxene-spinifex texture; includes medium-grained layers and lenses; minor interflow sedimentary rocks; metamorphosed; Fine-grained mafic schist; locally hornfelsed, amphibolitized or epidotized.|
77936|Hickies Bore Basalt|73151|5|Briefly described|p3, p10, p12 Tb.3|Neoarchean|Neoarchean|Yilgarn Craton. Kalgoorlie Terrane, Agnew Greenstone Belt.||Kalgoorlie Group||Overlies Donegal Komatiite, underlies Fourteen Mile Well Formation.|Basalt.|
77936|Hickies Bore Basalt|73596|6|Mentioned|p1151-1153, 1157, 1161-1163, 1167|||Lawlers Domain, Agnew-Wiluna Greenstone Belt. Deep-water mafic-ultramafic lava fields and feeder intrusions. Is intruded by a 2696 +/- 7 Ma granodiorite.||||Overlies Donegal Komatiite. Is overlain by Songvang Basalt. Lateral facies equivalent of lower McFarlanes Basalt.||
75577|Hidden Basin beds|65074|4|Described|p351 fig 4-37, p351, p353, p357 Tb. 4-12|Neoproterozoic|Neoproterozoic|See also p358, p360. Of SW Birrindudu Basin. 3 km thick. Type Section: 23 km SW of Lake Hazlett, 21o40'S, 128o25'E. Has broad and tight folds and faulting.||||Overlies Erica Sandstone unconformably(?).|Quartz arenite, sublithic arenite; lesser shale, siltstone.|
75577|Hidden Basin beds|69440|5|Briefly described|p25:1, 3|Cryogenian|Cryogenian|Occurs in STANSMORE and WEBB map areas. Up to 3000m thick. Forms parallel strike ridges. May conformably overlie Erica Sandstone, but the contact is hidden or faulted. Forms the top of the Murraba Basin succession.|||||Resistant quartz arenite and sublithic arenite; some thinly-bedded to laminated shale.|12-JUL-16
75577|Hidden Basin beds|70762|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|North Australian Craton.|||||Quartz sandstone, sublithic sandstone, shale and siltstone.|
75577|Hidden Basin beds|70826|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|Aileron Province.||||May be correlative of the Birrindudu Group.||
75577|Hidden Basin beds|71080|4|Described|p1,p4, 5, 7-8, 21-23, 26, 11, 28, 29, 32|Mesoproterozoic|Mesoproterozoic|Previously considered Murraba Basin, but may be part of older Birrindudu Basin.  Name derived from Hidden Basin, a large depression containing Lake Wills and Lake Hazlett. Previously believed to be Neoproterozoic and younger than Erica Sandstone. Observed in nominated reference area and 19 km further north. Divided into 5 local informal units to facilitate description. Paleocurrent flow towards the north (015deg). Induration, structural observations and geophysics all suggest this unit is older than other units in region. Previously included in Gardiner Beds.||||May be equivalent to Birrindudu Group rocks.|Base mainly red-brown medium-grained ferruginous sandstone;  central part not exposed; upper part mainly white to grey, medium grained, very well-silicified quartz sandstone, alternating thick bedded massive & thinner bedded flaggy intervals.|04-FEB-19
75577|Hidden Basin beds|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, shale, sandstone|
75577|Hidden Basin beds|72034|5|Briefly described|500k_interpgeop16_lut|Neoproterozoic|Paleoproterozoic||||||Quartz sandstone, sublithic sandstone, shale and siltstone.|
75577|Hidden Basin beds|73445|5|Briefly described|p3, 6-7, 10, 12-14, 23-24, 28, 34-35, 38|Mesoproterozoic|Mesoproterozoic|See also p41, 43-47, 51, 53, 56, 58, 65-118. Over 3,000m thick. More deformed and likely to be older than Redcliff Pound Group. Whole-rock and regolith chemistries tabulated. Multi-element spider diagram.|||||Sandstone, minor siltstone, and shale.|
80117|Hidden Secret Sandstone|71212|6|Mentioned|App.G p20|||Lawlers Prospect/Hidden Secret Prospect. [p709 of digital version of whole report]. Svetlana Sandstone mistaken for this unit.||||||26-SEP-17
80014|High Cliff Sequence|69297|6|Mentioned|p204, p223, p236|Artinskian|Sakmarian|Offshore Perth Basin. Same figure repeated p204, 223, 236.||||Overlies the Holmwood Sequence on Beagle Ridge.Overlain by the Irwin River Sequence in Abrolhos Sub-basin and Beagle Ridge.||20-SEP-17
79355|Highway Formation|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).  See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2726-2680 Ma (inferred)|Unit of Broad Arrow Subgroup.|||Amphibolite and metabasalt derived from mafic volcanics; basalt: pillowed to massive, variolitic, pyroxene spinifex-textured, metamorphosed; ultramafic schist; includes talc--chlorite(-carbonate) and tremolite-chlorite schist; peridotite.|
79355|Highway Formation|73596|6|Mentioned|p1162|||Broad Arrow Inlier, Kalgoorlie Terrane.||Broad Arrow Subgroup.||Overlies Scotia Basalt. Is overlain by Black Flag Group.||
80015|Holmwood Sequence|69297|6|Mentioned|p204, p223, p236|Sakmarian|Sakmarian|Offshore Perth Basin. Same figure repeated on all threee pages.||||Overlies the Nangetty Sequence, overlain by the High Cliff Sequence, in the Beagle Ridge area.||20-SEP-17
72356|Homeward Bound Granite|63417|5|Briefly described|Map legend|Archean|Archean|Of the Callina Supersuite. Age: c.3465Ma.  Geological Province: Pilbara Craton. Subvolcanic intrusions of porphyritic rhyolite and dacite, euhedral feldspar and quartz phenocrysts; typically in dark grey fine-grained to glassy matrix; metamoprhosed.||||||07-NOV-08
72356|Homeward Bound Granite|64621|5|Briefly described|Map legend|Archean|Archean|Of the Callina Supersuite. Age: c.3466Ma. Alkali-feldspar granite; medium- to coarse-grained; includes local diorite and granodiorite; massive to weakly foliated; metamorphosed.||||||07-NOV-08
72356|Homeward Bound Granite|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c.3465 Ma.|Of Callina Supersuite.|||Porphyritic microgranite and microgranodiorite, mainly in subvolcanic intrusions; euhedral feldspar and quartz phenocrysts typically in a dark grey, fine-grained to glassy matrix; metamorphosed.|
72356|Homeward Bound Granite|65827|4|Described|p6 Tb.2, p18|Paleoarchean|Paleoarchean|Of Callina Supersuite. c. 3465 Ma. Intrudes Duffer Formation. Variably metamorphosed, fine-grained, gneissic muscovite-bearing syenogranite with large elongate quartz lenses and microcline augen in a fine-grained quartz and alkali feldspar matrix.||||||
72356|Homeward Bound Granite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Callina Supersuite. Aged c.3466 Ma. Alkali-feldspar granite; medium- to coarse-grained; massive to weakly foliated; includes local diorite and granodiorite; weakly metamorphosed.||||||
72356|Homeward Bound Granite|66217|5|Briefly described|p24. |||A subvolcanic intrusion to the Duffer Formation.||Unit in Callina Supersuite.|||Alkali granite.|
72356|Homeward Bound Granite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Callina Supersuite|||Alkali-feldspar granite; medium- to coarse-grained; includes local diorite and granodiorite; massive to weakly foliated; includes local diorite and granodiorite; weakly metamorphosed|
72356|Homeward Bound Granite|69301|4|Described|p5 Fig.3, p8|||Pilbara Craton. East Pilbara Terrane. Geochronology has confirmed a previous interpretation (Reynolds et al. 1975; Hickman & Lipple 1978) that Homeward Bound Granite is a sub-volcanic intrusion associated with Duffer Formation. |3.466 Ga|Callina Supersuite||Intrudes Duffer Formation.||
72356|Homeward Bound Granite|69566|6|Mentioned|p236|||Mount Edgar Granitoid Complex, East Pilbara Granite-Greenstone Terrane.||Callina Supersuite.||||
72356|Homeward Bound Granite|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3466-3462 Ma (isotopic)|Unit of Callina Supersuite.||In fault contact with Fig tree Gneiss.|Alkali-feldspar granite; medium- to coarse-grained; includes local diorite and granodiorite, porphyritic microgranite and microgranodiorite, granitic rocks interlayered with mafic amphibolite.|
72356|Homeward Bound Granite|70733|6|Mentioned|p106||||3465 Ma.|||||
72356|Homeward Bound Granite|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||alkali feldspar granite, diorite, granodiorite, amphibolite|
72356|Homeward Bound Granite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||3466+/-2 Ma.|Callina Supersuite|||Alkali-feldspar granite; medium to coarse grained; includes local diorite and granodiorite; massive to weakly foliated; weakly metamorphosed.|
28109|Honeyeater Basalt|23416|5|Briefly described|Map Legend|Archean|Archean|Of Gorge Creek Group, Pilbara Craton.||||||22-APR-09
28109|Honeyeater Basalt|23755|4|Described|p44|Archean|Archean|See also page 17 table 1.  Of Gorge Creek Group.||||||07-NOV-08
28109|Honeyeater Basalt|23783|5|Briefly described|p17|||Of Gorge Creek Group.||||||
28109|Honeyeater Basalt|24025|4|Described|p8 Tb. 1|Archean|Archean|Of Gorge Creek Group.  Pillowed tholeiitic basalt and minor high-Mg basalt.  Max. thickness: 1000m. Geological Province: Pilbara Craton.||||||22-APR-09
28109|Honeyeater Basalt|24184|5|Briefly described|p702, p699 Fig.3|Archean|Archean|Parent: Gorge Creek Group. Overlying Unit: Pyramid Hill Formation. Underlying Unit: Paddy Market Formation. Geological Province: Pilbara Craton. Intruded by ultramafic and mafic sills of Dalton Suite.||||||07-NOV-08
28109|Honeyeater Basalt|24185|5|Briefly described|p747|Archean|Archean|Geological Province: Pilbara Craton. Parent: Gorge Creek Group.||||||07-NOV-08
28109|Honeyeater Basalt|24531|6|Mentioned|p51|||On the MUCCAN sheet.||||||
28109|Honeyeater Basalt|24550|5|Briefly described|p31 Tb. 3.1|||Of the Gorge Creek Group. Basalt. Geological Province: Pilbara Craton.||||||07-FEB-11
28109|Honeyeater Basalt|31853|2|Defined|p62|Archean|Archean|Supersedes Honeyeater Formation (defn never published).||||||07-NOV-08
28109|Honeyeater Basalt|37373|4|Described|p79|||||||||
28109|Honeyeater Basalt|38498|5|Briefly described|Table 1|||||||||
28109|Honeyeater Basalt|38544|6|Mentioned|Fig.1|||||||||
28109|Honeyeater Basalt|39444|6|Mentioned|Table 1|||||||||
28109|Honeyeater Basalt|39697|4|Described|p100|||||||||
28109|Honeyeater Basalt|41252|6|Mentioned|p50|||||||||
28109|Honeyeater Basalt|43595|6|Mentioned|p213|||||||||
28109|Honeyeater Basalt|43698|6|Mentioned|p3|||||||||
28109|Honeyeater Basalt|43779|5|Briefly described|p7|||||||||
28109|Honeyeater Basalt|44150|5|Briefly described|p129 Tb.2-15, p132 Fig.2-131, p135|||See also p139 Tb.2-18, p152 Tb.2-22. Less than 1km thick.||Gorge Creek Group|||Tholeiitic basalt; minor high-Mg pillow basalt; both intruded by dolerite and gabbro sills. Metamorphosed to prehnite-pumpellyite facies.|
28109|Honeyeater Basalt|46922|6|Mentioned|p259|||Trace element analysis.||||||
28109|Honeyeater Basalt|50544|6|Mentioned|p41|||Equivalent to the Coonieena Basalt (Gorge Creek Group).||||||
28109|Honeyeater Basalt|60429|6|Mentioned|p18|||Mafic volcanic rocks.||||||07-FEB-11
28109|Honeyeater Basalt|61253|5|Briefly described|p51|Archean|Archean|Of the Gorge Creek Group.  Geological Province: Pilbara Craton.||||||07-NOV-08
28109|Honeyeater Basalt|61266|5|Briefly described|p58 Tb.1|Archean|Archean|Of the Gorge Creek Group. Geological Province: Pilbara Craton.||||||07-NOV-08
28109|Honeyeater Basalt|61579|5|Briefly described|p58 Fig. 2|Archean|Archean|Of the Gorge Creek Group.||||||07-NOV-08
28109|Honeyeater Basalt|63441|4|Described|p4 Tb. 1, p22|Archean|Archean|Of the Soanesville Group (Pilbara Supergroup). Conformably (or disconformably?) overlies Paddy Market Formation; conformably overlain by Pyramid Hill Formation. Max. thickness: ~900m. Geological province: Pilbara Craton. Of basalt and komatiitic basalt.||||||07-FEB-11
28109|Honeyeater Basalt|63538|4|Described|p5, p10, p16, p6 Fig. 3|Archean|Archean|Of Soanesville Group. Underlain by Paddy Market Formation, overlain by Pyramid Hill Formation. Komatiitic basalt and banded iron-formation. Geological Province: Pilbara Craton. Mafic volcanic rocks.||||||19-APR-13
28109|Honeyeater Basalt|64328|5|Briefly described|p56 Tb. 1|||||||||07-FEB-11
28109|Honeyeater Basalt|64384|5|Briefly described|p26 Tb. 3|Archean|Archean|Of the Gorge Creek Group. Max. thickness:1km.||||||07-FEB-11
28109|Honeyeater Basalt|64405|5|Briefly described|p4 Fig. 3|Archean|Archean|Name inferred from Honeyeater only in Figure 3. Of the Soanesville Group (De Grey Supergroup).||||||07-FEB-11
28109|Honeyeater Basalt|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Unit in Soanesville Group. Massive and pillowed basalt and komatiitic basalt; locally vesicular; metamorphosed.||||||
28109|Honeyeater Basalt|66118|4|Described|p147, p149 Fig.3, p152, p154-155, p159|||Pilbara Craton. East Pilbara Terrane. Soanesville greenstone belt. Thickness: 1000-2000 m. Dalton Suite subvolcanic sills interpeted as from Honeyeater Basalt. Intrusive Dalton Suite age (3182+/-2 Ma gabbro SHRIMP U-Pb zircon) interpreted as igneous emplacement age of sill as well as eruptive age of associated Honeyeater Basalt (Soanesville Group).|3182+/-2 Ma Dalton Suite gabbro SHRIMP U-Pb zircon|Near top of Soanesville Group||Is intruded by Dalton Suite. Is overlain by Pyramid Hill Formation in Soanesville greenstone belt.|Well preserved, weakly metamorphosed (prehnite-pumpellyite grade) pillow basalts with common marginal vesicles and local varioles; typically low-Ti basalts and komatiitic basalts with strongly LREE-depleted normalized trace-element patterns.|
28109|Honeyeater Basalt|66745|6|Mentioned|pp52-53.|Mesoarchean|Mesoarchean|||Constitutes the upper part of Soanesville Group.||Overlies Paddy Market Formation. Is overlain by Pyramid Hill Formation.||
28109|Honeyeater Basalt|67130|5|Briefly described|p16|||1150m thick, eruption was accompanied with emplacement of Daltons Suite.||Soanesville Group||Overlies Paddy Market Formation, overlain by Pyramid Hill Formation|Basalt.|
28109|Honeyeater Basalt|67197|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Soanesville Group.||||
28109|Honeyeater Basalt|67201|4|Described|p7 Fig.4, p12 Tb.1|||In northern Pilbara Craton, East Pilbara Terrane, Soanesville Basin, rift-related successions.|c. 3180 Ma|Soanesville Group||||
28109|Honeyeater Basalt|67269|5|Briefly described|p5|Paleoarchean|Paleoarchean|||Soanesville Group.|||Basalt.|
28109|Honeyeater Basalt|67668|6|Mentioned|Fig. 2; p. 154||Mesoarchean|East Pilbara Terrane, Pilbara Craton.||Soanesville Group||Underlies the Pyramid Hill Formation and overlies the Paddy Market Formation.||
28109|Honeyeater Basalt|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Soanesville Basin. Mapped as 8 separate facies.||Of the Soanesville Group.|||Amphibolite, silicified metabasalt, metakomatiitic basalt, silicified mafic schist, tremolite-chlorite-talc schist, interlayered ultramafic schist and quartzite, and metamorphosed basalt.|30-APR-14
28109|Honeyeater Basalt|69015|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton. Includes 4 unnamed sub-units mapped separately.||Of the Soanesville Group.|||Massive and pillowed basalt and komatiitic basalt, locally vesicular; schist derived from metabasalt; layered chert; basalt; komatiitic basalt, locally pillowed; all metamorphosed.|02-MAY-14
28109|Honeyeater Basalt|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Soanesville Group|||Massive and pillowed basalt and komatiitic basalt; locally vesicular; metamorphosed. Amphibolite, metabasalt, schist, silicified mafic schist, tremolite-chlorite-talc schist, interlayered quartzite. Layered metachert, metakomatiitic basalt.|
28109|Honeyeater Basalt|69301|5|Briefly described|p5 Fig.3, p9 Tb.1|||Pilbara Craton. East Pilbara Terrane. Soanesville Basin. Rift-related successions.|3180 Ma|Soanesville Group||||
28109|Honeyeater Basalt|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Paleoarchean|Geological province: Pilbara Craton. Of Soanesville Basin. Events: Mosquito Creek Orogeny; North Pilbara Orogeny; Prinsep Orogeny; East Pilbara Terrane Rifting Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.|3228-3176 Ma (inferred)|Unit of Soanesville Group.|||Amphibolite and schist derived from basaltic rocks, (meta)basalt; komatiitic, massive, pillowed; interlayered ultramafic schist and quartzite.|
28109|Honeyeater Basalt|69616|5|Briefly described|p161, p162-163 Fig.3, p180, p183|Archean|Archean|Maximum thickness 900m.||Unit in Soanesville Group.||Overlies Paddy Market Formation. Is overlain by Pyramid Hill Formation.|Basalt and komatiitic basalt.|
28109|Honeyeater Basalt|70022|6|Mentioned|p115|||East Pilbara Terrane.||Soanesville Group.||||
28109|Honeyeater Basalt|70775|5|Briefly described|p6, p12|||Soanesville Basin. ||Soanesville Group||Overlies the Paddy Market Formation. Faulted against the Regal Formation.|Pillow Basalt.|
28109|Honeyeater Basalt|71041|4|Described|p44, p45 fig 2, p47 fig 4|Mesoarchean|Mesoarchean|Contains basalts and BIFs that were previously assigned to the Euro Basalt and the Corboy Formation. |3180 Ma|Soanesville Group||Unconformably overlain by the Cleaverville Formation. Intruded by the Dalton Suite.|Mafic volcanosedimentary rocks.|
28109|Honeyeater Basalt|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Paleoarchean|Soanesville Basin.||Soanesville Group|||Massive and pillowed basalt and komatiitic basalt; locally vesicular; metamorphosed.|
28109|Honeyeater Basalt|72251|5|Briefly described|p54|Mesoarchean|Mesoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Soanesville Group.||Overlain by Pyramide Hill Formation, or unconformably by Farrel Quartzite. Underlain by Paddy Market Formation.||
28109|Honeyeater Basalt|72668|5|Briefly described|p4-7, p28|||East Pilbara Terrane. 1150m thick. Associated with the Daltons Suite of layered mafic-ultramafic intrusions.||Soanesville Group||Overlies the Paddy Market Formation. Overlain by the Pyramid Hill Formation.|Komatiitic and tholeiitic pillow basalts.|13-JAN-22
28109|Honeyeater Basalt|73598|6|Mentioned|p1212|Mesoarchean|Mesoarchean|East Pilbara Terrane.||Soanesville Group.||Overlies Paddy Market Formation. Is overlain by Pyramid Hill Formation.||
37897|Honeymoon Well ultramafic complex|24135|6|Mentioned|p30|||Informal name.||||||
75921|Hope Campbell Orthogneiss|66113|5|Briefly described|Map legend|Archean|Archean|Burtville Terrane, Yilgarn Craton. Unit in Minigwal Suite. Age c.2769 Ma. Migmatitic quartz-biotite orthogneiss.||||||
75921|Hope Campbell Orthogneiss|68107|5|Briefly described|p609 Tb.1.|Neoarchean|Neoarchean||2769 +/- 8 Ma (Wingate et al. 2010).|Of the Minigwal Suite.|||Orthogneiss.|22-SEP-14
75921|Hope Campbell Orthogneiss|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Burtville Terrane, Eastern Goldfields Superterrane, Yilgarn Craton. Magmatic crystallization age of the tonalitic precursor to the orthogneiss: 2769+/-8 Ma. See geochron files 193360.1.pdf, 193361.1.pdf (2010).||Minigwal Suite||Intruded by Balpe Lakes Monzogranite.|Migmatitic quartz-biotite orthogneiss.|06-AUG-15
75921|Hope Campbell Orthogneiss|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|See also 100k_geologyp14_lut.csv and 500k_interpgeop14_lut.csv. Age derived from orthogneiss sample (193360.1.pdf) and constrains magmatic crystallization age of the tonalitic precursor to the orthogneiss.|2769 Ma +/-8 Ma (SHRIMP)|Minigwal Suite|||Migmatitic quartz-biotite orthogneiss.|
75921|Hope Campbell Orthogneiss|70802|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Burtville Terrane, Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events.|2769+\-8 Ma; 2765 Ma (inferred)|Unit of Minigwal Suite.|||Migmatitic quartz-biotite orthogneiss|
75921|Hope Campbell Orthogneiss|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Burtville Terrane, Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma). Sample GSWA 193360 (orthogneiss) yielded a weighted mean 207Pb/206Pb date of 2769+\-8 Ma, interpreted to be magmatic crystallisation age of the tonalitic precursor to the orthogneiss. See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 100k_geologyp14_lut.csv, 500k_interpgeop_lut.csv.|2769+\-8 Ma; 2765 Ma|Unit of Minigwal Suite.|||Migmatitic quartz-biotite orthogneiss.|
75921|Hope Campbell Orthogneiss|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Burtville Terrane.|Max age 2769+/-8 Ma, min ~2765 Ma.|Minigwal Suite|||Migmatitic quartz--biotite orthogneiss|
80118|Horse Paddock Leucogranite|71212|5|Briefly described|p85, 86, p90, p136, p72|||Yilgarn Craton. Outcrop characteristics discussed. Named for the Horse Paddock Well. See also p53 where it is referred to as the Horse Paddock Monzogranite.|||||Medium-grained, weakly foliated` and leucocratic granite with a very low abundance of mafic minerals.|26-SEP-17
80118|Horse Paddock Leucogranite|73151|6|Mentioned|p3-4|||Yilgarn Craton. Older basement or inherited age of 2797 +/- 8 Ma, Geoscience Australia Geochronology Laboratory (2007).|||||Leucogranite.|
27801|Horseshoe Formation|7161|5|Briefly described|p92 Fig.4, p94|||Horseshoe Basin. Approximately 1000m thick (from p92 Fig.4).||||Underlain by the Johnson Cairn Shale.|Carbonate cemented, quartzofeldspathic rhythmites and chloritic laminites; laminated Fe-rich shale, Mn-oxide and Mn-carbonate diagenetic alteration; siliciclastic rhythmites and organic-rich shale, Mn-oxide and Mn-carbonate diagenetic alteration.|02-MAY-12
27801|Horseshoe Formation|12099|4|Described|p678 Fig.4, p680-1, p683, 685|Orosirian|Orosirian|Placed in Glengarry Group by Gee (1987). Approximately 1km thick at type locality in the Horseshoe Range.||Unit in Bryah Group.||In faulted contact with Narracoota Formation. Conformably overlies Ravelstone Formation. Locally unconformably overlain by Padbury Group.|Contains finely laminated hematitic shale and siltstone, fine-grained quartz-feldspar wacke with interleaved iron-formation and chert, graded quartz wacke, manganiferous shale, garnetiferous biotite-chlorite schist, and garnetiferous iron-formation.|04-MAR-13
27801|Horseshoe Formation|22493|6|Mentioned|p92|||||||||
27801|Horseshoe Formation|22694|5|Briefly described|p7|||Bryah Group||||||
27801|Horseshoe Formation|22940|4|Described|p16, Fig.1 p3, Fig.6 p14|Paleoproterozoic|Paleoproterozoic|See also Table 2 p12. of Bryah Group.||||||07-NOV-08
27801|Horseshoe Formation|23151|5|Briefly described|p67|||of Bryah Group.||||||
27801|Horseshoe Formation|23592|5|Briefly described|p12|||Of Bryah Group. Geological Province: Bryah Basin.||||||
27801|Horseshoe Formation|23593|5|Briefly described|p2 Fig 1|||Of Bryah Group. Geological Province: Bryah Basin||||||
27801|Horseshoe Formation|23600|5|Briefly described|p4 Fig 2|||Of Bryah Group. Geological Province: Bryah Basin.||||||
27801|Horseshoe Formation|23744|4|Described|p13|Paleoproterozoic|Paleoproterozoic|Of Bryah Group. Geological Province: Bryah Basin. Max. thickness: 1000 m.||||||07-NOV-08
27801|Horseshoe Formation|23747|4|Described|p14|Paleoproterozoic|Paleoproterozoic|See also page 9, p4 table 1. Of Bryah Group. Geological Province: Bryah Basin.||||||07-NOV-08
27801|Horseshoe Formation|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Bryah Group. Geological Province: Bryah Basin||||||
27801|Horseshoe Formation|23749|5|Briefly described|p3 table 1|Proterozoic|Proterozoic|Of Bryah Group. Geological Province: Bryah Basin.||||||
27801|Horseshoe Formation|23798|6|Mentioned|p3|||Mixed sediments. Geological Province: Yilgarn Craton. See also Horseshoe formation.||||||05-JUL-06
27801|Horseshoe Formation|23890|5|Briefly described|p21 Fig.11|||Of Bryah Group. Geological Province: Bryah Basin.||||||
27801|Horseshoe Formation|24021|5|Briefly described|p3, Fig. 1|||Parent: Bryah Group.||||||
27801|Horseshoe Formation|35975|3|Fully described|p103|||||||||
27801|Horseshoe Formation|40937|6|Mentioned|p29|||||||||
27801|Horseshoe Formation|40938|5|Briefly described|p11|||Mention Fig.5||||||
27801|Horseshoe Formation|40989|4|Described|p24|||||||||
27801|Horseshoe Formation|42260|6|Mentioned|p125|||||||||
27801|Horseshoe Formation|42730|5|Briefly described|Fig 12, P15|||||||||
27801|Horseshoe Formation|43069|5|Briefly described|Fig.2|||of Glengarry Group||||||
27801|Horseshoe Formation|43238|4|Described|p6|||Of Bryah Group.||||||09-DEC-08
27801|Horseshoe Formation|43830|5|Briefly described|Map Legend||Paleoproterozoic|Bryah Basin||||||07-NOV-08
27801|Horseshoe Formation|43831|5|Briefly described|Map Legend||Paleoproterozoic|Bryah Basin||||||07-NOV-08
27801|Horseshoe Formation|49893|6|Mentioned|p2 Fig.1|||Of the Bryah Group.||||||
27801|Horseshoe Formation|49896|5|Briefly described|p2 Tb. 1|||Of Gee (1979a). Initially Horeshoe Range Beds, then H.R. Formation, then H.R. Beds and now Horseshoe Range Formation again (Occhipinti 1997). Of the Bryah Group.||||||
27801|Horseshoe Formation|50222|4|Described|p325|Paleoproterozoic|Paleoproterozoic|Of the Bryah Group.  Conformably overlies the Ravelstone Formation.  Max. thickness: ~1000m.   Geological Province: Bryah Basin.||||||07-NOV-08
27801|Horseshoe Formation|50226|5|Briefly described|p421 Fig. 4, p422|||Of the Bryah Group.  Overlies Narracoota Formation.  Geological Province: Bryah Basin.||||||09-DEC-04
27801|Horseshoe Formation|61217|5|Briefly described|p43 Fig. 2A|Proterozoic|Proterozoic|Mixed sediments and wackes - calcareous, manganiferous shales and subgreywackes.||||||07-FEB-11
27801|Horseshoe Formation|61271|6|Mentioned|p105 Fig.1, p107|||Of the Bryah Group.||||||27-MAY-06
27801|Horseshoe Formation|61848|5|Briefly described|p300|||Turbiditic metasedimentary rocks, BIF and associated clastic sediments - including calcareous manganiferous shales and subgreywackes. Geological Province: Bryah Basin.||||||
27801|Horseshoe Formation|62289|6|Mentioned|p4 Fig. 2|Palaeoproterozoic|Palaeoproterozoic|Of Bryah Group. Occhipinti et al. (1997); Piranjo et al. (1998c), and this study||||||
27801|Horseshoe Formation|63866|5|Briefly described|p164|||Western Glengarry Basin.||Bryah Group||||
27801|Horseshoe Formation|64384|5|Briefly described|p78 Tb. 8|||Of the Glengarry Group. Geological province: Glengarry Sub-basin. Greywacke, shale, BIF.||||||07-FEB-11
27801|Horseshoe Formation|64580|4|Described|map legend||Paleoproterozoic|Of Bryah Group. Sandstone; minor shale and conglomerate.||||||09-DEC-08
27801|Horseshoe Formation|64724|6|Mentioned|p43|Orosirian|Orosirian|||Of Bryah Group.||||02-APR-12
27801|Horseshoe Formation|65408|5|Briefly described|pp82-83.|Paleoproterozoic|Paleoproterozoic|||Unit in Bryah Group.|||Chemical and fine-grained clastic units: BIF, wacke, shale.|
27801|Horseshoe Formation|65411|5|Briefly described|p88, p91, p94.|Paleoproterozoic|Paleoproterozoic|Forms an anticlinal fault-block.||Topmost unit in Bryah Group.||Is overlain unconformably by Padbury Group.|Shale, banded iron-formation.|
27801|Horseshoe Formation|65412|6|Mentioned|p97 Fig.1.|Paleoproterozoic|Paleoproterozoic|||||||
27801|Horseshoe Formation|65419|1|Redefined|p4 Fig.1, pp35-36.|Paleoproterozoic|Paleoproterozoic|Includes strata previously referred to as the Horseshoe Range Beds by MacLeod (1970), Barnett (1975) and Elias and Williams (1980); and the Horseshoe Formation by Gee (1979, 1985). Named after the Horseshoe Range. No type section; type area is 'a section extending for 3 km west from the Horseshoe goldmine across the Horseshoe Range' (Gee 1979). Thickness is c.750 m.||Unit in Bryah Group.||Overlies Ravelstone Formation conformably and gradationally. Is faulted against the Narracoota Formation. Is overlain unconformably by Labouchere Formation.|Sericitized quartz wacke, and manganiferous shale with intercalated banded iron-formation which is garnetiferous in the Horseshoe Range.|
27801|Horseshoe Formation|65896|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Top unit in Bryah Group. Ferruginous, chloritic shale and quartz-feldspar wacke; partly manganiferous and calcareous; includes iron-formation and chert; metamorphosed.||||||
27801|Horseshoe Formation|65913|6|Mentioned|p2 Fig.1. |||||Unit in Bryah Group.||||
27801|Horseshoe Formation|66112|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Bryah Group. Ferruginous, chloritic shale, and quartz-feldspar wacke; partly manganiferous and calcareous; includes iron formation and chert.||||||
27801|Horseshoe Formation|67855|5|Briefly described|p204 tab 3-1|Paleoproterozoic|Paleoproterozoic|Gascoyne Complex, Nabberu Basin. 1km thick iron formation-sandstone-shale basin-fill facies||Glengarry Group||||
27801|Horseshoe Formation|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic|||Bryah Group|||ferruginous, chloritic shale and quartz-feldspar wacke; partly manganiferous and calcareous; includes iron formation and chert; metamorphosed|
27801|Horseshoe Formation|69003|5|Briefly described|p11-14|||Bryah Basin. 750m thick. Post-rift-fill succession.||Bryah Group.||Conformably overlies Ravelstone Formation.|Fine-grained argillites and ironstones.|
27801|Horseshoe Formation|69010|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Bryah Basin. An unnamed sub-unit of quartz-magnetite-(stilpnomelane) iron formation with white chert lenses is mapped separately.|2014-1983 Ma|Of the Bryah Group.|||Comprises ferruginous, chloritic shale, and quartz-feldspar wacke; partly manganiferous and calcareous; includes iron formation and chert.|24-APR-14
27801|Horseshoe Formation|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|||Bryah Group|||Ferruginous, chloritic shale, and quartz--feldspar wacke; partly manganiferous and calcareous; includes iron formation and chert|
27801|Horseshoe Formation|69583|5|Briefly described|Plate 2|Proterozoic|Proterozoic|Bryah Basin.|c.2000 Ma.|Bryah Group.|||Ferruginous, chloritic shale and quartz-feldspar wacke.|
27801|Horseshoe Formation|69596|6|Mentioned|p10-11|||Bryah Basin.||||Conformably overlies Ravelstone Formation.|Predominantly fine-grained siliciclastic and chemical rocks including interbedded siltstone and shale, wacke, and iron-formation.|
27801|Horseshoe Formation|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv, West Australian Craton, Bryah Basin|2014-1920 Ma|Bryah Group|||Ferruginous, chloritic shale and quartz-feldspar wacke; partly manganiferous and calcareous. Iron formation and chert.|
27801|Horseshoe Formation|70796|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|Bryah Basin, Capricorn Orogen.|2014  1920 Ma (inferred)|Bryah Group, upper|||Ferruginous, chloritic shale, and quartzfeldspar wacke; partly manganiferous and calcareous; includes iron formation and chert.|
27801|Horseshoe Formation|70804|5|Briefly described|p2, p6-p8, p11, p16-p18|||The type area is located in the Horseshoe Range (Occhipinti et al, 1997) where a thickness of approximately 1000m was estimated. A stratigraphic column is provided from approximately 1km north of the Ravelstone manganese deposits. See also p24-p26, p28, p38, p44, plate 1.||Bryah Group||Conformably overlies the Ravelstone Formation. Overlies (conformably or tectonically) the Narracoota Formation. Unconformably overlain by the Labouchere Formation.|Finely laminated ferruginous shale and siltstone, fine-grained quartz-feldspar wacke with interleaved iron formation and chert, graded quartz wacke, manganiferous shale, garnetiferous biotite-chlorite schist and garnetiferous iron-formation.|
27801|Horseshoe Formation|71042|6|Mentioned|p96|||Bryah Basin. This unit has historically been mined for manganese and iron.||Bryah Group||||
27801|Horseshoe Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||banded iron formation, greywacke, shale|
27801|Horseshoe Formation|71269|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen, West Australian Craton. Of Bryah Basin. Events: Capricorn Orogeny (1817-1772 Ma); Glenburgh Orogeny (2002-1947 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv.|2014-1920 Ma (inferred)|Unit of Bryah Group.|||Ferruginous, chloritic shale, and quartz--feldspar wacke; partly manganiferous and calcareous; includes iron formation and chert|
27801|Horseshoe Formation|71468|5|Briefly described|p24-25|Orosirian|Orosirian|Geological province: Capricorn Orogen, Yilgarn Craton. Of Bryah and Padbury sub-basins.||||Overlain by Padbury Group. Underlain by Ravelstone and Narracoota Formations.||
27801|Horseshoe Formation|71484|4|Described|p125,128-129,134-136,138|Orosirian|Orosirian|Geological province: Of Bryah Basin. Deposited in low-energy shallow water environment in which chemical sediments were precipitated in isolated depressions. Records the last basin fill of the Bryah Basin, marking the end of volcanism and volcanosedimentary deposition of the underying Ravelstone Formation. outboard correlative to the Maraloou Formation.||Unit of Bryah Group.||Uppermost unit of Bryah Group. Overlain unconformably by Labourchere Formation/Padbury Group. Underlain by Ravelstone Formation.|Ferruginous, chloritic shale and quartz-feldspar wacke, partly manganiferous and calcareous, iron formation and chert.|30-AUG-19
27801|Horseshoe Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Bryah Basin.||Bryah Group, upper|||Ferruginous, chloritic shale, and quartz--feldspar wacke; partly manganiferous and calcareous; includes iron formation and chert.|
81532|Horseshoe Supersequence|71112|5|Briefly described|p69-70|Paleoproterozoic|Paleoproterozoic|Geological province: Ashburton Province, Pilbara Craton. Of the Horseshoe Basin (intracontinental rift basin). Maximum age ~2145 Ma. Includes Beasley River Quartzite, Cheela Springs Basalt, Wooly Dolomite.||||Overlain by Mount McGrath Formation. Underlain by Turee Creek Group (>2208 +/-10 Ma)||30-AUG-19
74627|Horsewater Soak Calcarenite|64449|2|Defined|p75, p76, p79 Tb. 5, p103-106|Holocene|Holocene|Overlies Kennedys Cottage Limestone and Willie Creek Calcarenite. Underlies Shoonta Hill Sand. Thickness: 3m. Cross-laminated aeolian calcarenite; shoe-string deposit formed as earlier Holocene supratidal dunes.||||||07-FEB-11
74627|Horsewater Soak Calcarenite|73213|6|Mentioned|956 Fig.1, 958 Fig.3(b)|||||||Overlies Kennedys Cottage Limestone.||
23655|Hotham Formation|33800|2|Defined|p138|Archean|Archean|Type area on a ridge 4.8 km east-southeast of George Hill.Total thickness not exposed.|||||Well banded, silty metasediments, with minor pyroclastic units.|14-FEB-18
23655|Hotham Formation|37017|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
23655|Hotham Formation|40370|5|Briefly described|p7|||||||||
23655|Hotham Formation|40775|4|Described|p494|||||||||
23655|Hotham Formation|40785|6|Mentioned|Fig.1|||||||||
23655|Hotham Formation|42165|5|Briefly described|p92|||||||||
23655|Hotham Formation|64016|6|Mentioned|p12, p12 Fig. 4|||Metasediments.||||||
76029|Hoult Sandstone Member|69558|4|Described|p106, p110 fig 167, p260, p262|Pleistocene|Pleistocene|Named for the Hoult Landing on Faure Island. Previously referred to as the Faure Sandstone Member, though this was inappropriate as there was already a Faure Formation in the area. Contains a rich bivalve and gastropod fossil assemblage. Dips east at 2 degrees.Type section location noted.||Peron Sandstone|||Fossiliferous, reddish-yellow, calcareous sandstone.|25-MAY-21
38357|Hovea Member|60377|4|Described|p61 Fig. 3, p64-74|Scythian|Wuchiapingian|Of the Kockatea Shale. Underlain by Dongara Sandstone and Beekeeper Formation. Geological Province: Perth Basin. Marine depositional environment. Consists of carbonaceous shales.||||||07-FEB-11
38357|Hovea Member|60420|5|Briefly described|p423-425, Fig. 2|Early Triassic|Late Permian|At base of the Kockatea Shale. Max. thickness: 27.7m. Forms the impermeable cap rock for the Dongara Sandstone. Fossiliferous black mudstone, sandy siltstone and shelly storm beds. Limestone, laminated mudstone.||||||27-SEP-07
38357|Hovea Member|61541|5|Briefly described|pp263-270.|Griesbachian|Changhsingian|Perth Basin. Contains excellent oil source rocks; a distinctive zone enriched in organic matter (TOC up to 5%) called the Sapropelic Interval. Deposition in a shallow shelf during end-Permian global marine transgression due to a global warming interval, accompanied by an oceanic anoxic event.||Basal unit in Kockatea Shale.|||Variably bioturbated siltstones and fine sandstones, overlain by laminated mudstones and siltstones with occasional limestones.|
38357|Hovea Member|61546|5|Briefly described|p383.|Late Permian|Late Permian|Believed to be the principal oil-prone source rock in the Perth Basin. Deposited during a marine transgression.||Unit in Kockatea Shale.||||
38357|Hovea Member|61811|6|Mentioned|p20, p63.|Early Triassic|Early Triassic|Tentatively correlated with stromatolitic layer of Kockatea Shale. Type section details in Appendix 1.||||||
38357|Hovea Member|64099|5|Briefly described|p365, p367 Fig 2, p368, p373, p374 Fig 5|Olenekian|Wuchiapingian|At base of Kockatea Shale. The P-T boundary is placed within the lower part of the Sapropelic Interval within this unit, using palynological evidence and correlation of other stratigraphic units in Australia and China. Geol Prov: northern Perth Basin.||||||
38357|Hovea Member|67370|4|Described|pp315-319, p325, p328.|Early Triassic|Late Permian|The base of this unit contains a P. microcorpus Oppel Zone, and possibly D. parvithola Oppel Zone. Both were included in the Late Permian by Thomas and Barber (2004). The sapropel interval in its upper part contains distinctive Early Triassic bivalves, conodonts and ammonoids.||Basal unit in Kockatea Shale.|||Includes a sapropelic interval and an inertinitic interval.|
38357|Hovea Member|68202|6|Mentioned|p177|Triassic|Permian|The Permian-Triassic boundary is most likely at the junction of the Inertinitic and overlying Sapropelic intervals in this Member.||Basal Kockatea Shale.||||
38357|Hovea Member|69029|5|Briefly described|p330,332|Olenekian|Olenekian|Of Perth Basin. Laterallty extensive and hosts the best oil-prone source rocks in the Perth Basin. Marks the Permian-Triassic boundary extinction event associated with global source rock deposition (Thomas et al, 2004, Thomas and Barber, 2004).||Unit of Kockatea Shale.||||
38357|Hovea Member|69182|6|Mentioned|Ch2 p34-p41, Ch2 p46, Ch2 p99|||||||||
38357|Hovea Member|69297|6|Mentioned|p204-p206, p223, p236, p237, p515|Triassic|Triassic|Perth Basin. Is a potentially rich source rock, particularly on the Beagle Ridge and its vicinity. ||Kockatea Sequence. ||Overlain by the Kockatea Sequence.||
38357|Hovea Member|70097|5|Briefly described|p4, p6-7, p20 Fig.4|Early Triassic|Early Triassic|Initial slow deposition resulted in the accumulation of the organic-rich sediments of the Hovea Member (45.7 m thick in Lilac 1). This was followed by rapid deposition of the remainder of the Kockatea Shale (435 m thick in Batavia 1). Effective source rock constrained to an earliest Triassic, middle sapropelic interval, typically 10-40 m thick. Northern part of onshore and offshore Perth Basin. Northern Perth Basin. Dongara Saddle.||Kockatea Shale||Overlies Wittecarra Sandstone. Is overlain by Aranoo Sandstone Member.|Shale.|12-SEP-17
38357|Hovea Member|72505|5|Briefly described|p890|Induan|Changhsingian|Perth Basin. Correlates with the P. Microcorpus and P. Crenulata zones.||Kockatea Shale||Overlies the Beekeeper Formation and the Dongara Sandstone.||
38357|Hovea Member|73304|6|Mentioned|p71, p77|||Perth Basin. Permian-Triassic mass extinction level occurs in this unit at the boundary of inertinitic and sapropelic intervals.||Kockatea Shale||||
38357|Hovea Member|73484|5|Briefly described|p476 Fig.3, p487, p491|Early Triassic|Lopingian|Perth Basin. Marine. Contains an Inertinitic Interval at base, an overlying Sapropelic Interval, and a Limestone Marker of early Induan to early Olenekian age based on conodonts. Limestone marker had been tentatively correlated with northern Perth Basin Stromatolitic Sequence.||Kockatea Shale||Underlies Kockatea Shale||
38357|Hovea Member|73513|5|Briefly described|p30 Fig.2|Scythian|Tatarian|Perth Basin.||Kockatea Shale|||Marine rocks.|
31465|Hoya Formation|23523|4|Described|p994|Permian|Permian|Of Grant Group. See also p997. Geological Province: Canning Basin.||||||04-NOV-09
31465|Hoya Formation|43823|4|Described|p753|||First described in Barbwire Terrace area.||||||24-NOV-08
31465|Hoya Formation|64580|6|Mentioned|map legend|||Of Grant Group.||||||24-NOV-08
31465|Hoya Formation|64630|5|Briefly described|p31 Fig.2, p35, p37|Sakmarian|Sakmarian|N.B. Tentative ages, awaiting further palynology work for confirmation of dates. Province: subsurface Barbwire Terrace area of Canning Basin. Part of the Grant Group, underlies the Calytrix Formation. Palynology age: P. confluens.||||||19-OCT-09
31465|Hoya Formation|64643|5|Briefly described|p8|Sakmarian|Asselian|Of Grant Group across the Barbwire Terrace.||||||30-OCT-15
31465|Hoya Formation|64971|5|Briefly described|p684, p685 Fig. 2, p687, p689, p690|Early Permian|Early Permian|Of Grant Group. Geological Province: Canning Basin. Also on p691.||||||09-FEB-10
31465|Hoya Formation|66949|4|Described|p10-11, p13, p16-19; p46-48,51-54 Appx.2|Sakmarian|Asselian|See also p58 Appx.3, p60-65 Appx.4; p66-75,77,80-83,91-94 Appx.5; Plates 8-10,12. Type section in Pratia 1. Age from palynology.  Details given. Up to 250m thick; glacial shallow marine to fluvial deposits. Marked basal unconformity across the Barbwire Terrace is interpreted as a glacially eroded surface. Available core and Formation picks detailed.||Unit in Grant Group.||Unconformably overlies Tandalgoo Formation,  Reeves Formation. Is overlain conformably by Calytrix Formation.|Basal thick diamictites, mudstones and dropstones and massive sandstone.|05-NOV-15
31465|Hoya Formation|67354|5|Briefly described|pp106-107, p108 Fig.39.|||Possible equivalent to Blacktip Member of the Treachery Shale. Considered to be proximal sediments deposited following deglaciation.||||Is overlain by Calytrix Formation.||
31465|Hoya Formation|68007|5|Briefly described|p9|Permian|Permian|||Grant Group.||Equivalent to Betty Formation.||
31465|Hoya Formation|68656|6|Mentioned|GEOL_LUT_CSV/500k_geologyp08_lut|||||Grant Group||||
31465|Hoya Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Cisuralian|Pennsylvanian|||||||
31465|Hoya Formation|69297|6|Mentioned|p337, p352|Asselian|Gzhelian|Broome Platform of the Canning Basin. ||Grant Group||Overlies the Reeves Formation. Overlain by the Calytrix Formation.||
31465|Hoya Formation|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Grant Group.||||
31465|Hoya Formation|69693|5|Briefly described|p3, 10|Permian|Permian|Barbwire Terrace, Canning Basin. Asselian to Sakmarian.||Grant Group||Overlies Lower Grant Group. Is overlain by Calytrix Formation. Equivalent to Betty Formation.|Mixed sandstone and diamictite rich unit.|
31465|Hoya Formation|70774|5|Briefly described|p5 fig 3|Sakmarian|Asselian|Canning Basin.||Grant Group||Overlain by the Calytrix Formation.||
31465|Hoya Formation|72496|5|Briefly described|p217-220, p222, p230-231|Sakmarian|Asselian|Canning Basin, Barbwire Terrace. Contains abundant glacial material. Ranges in thickness from 82 to 417.5m; thickens by up to 227m in the Fitzroy trough and thins towards toe Lennard Shelf and Barbwire Terrace.||Grant Group||Equivalent to the Betty Formation. Overlain by the Calytrix Formation.|Fining upwards sequence of sandstone, sand and mud rich diamictite and mudstones.|
31465|Hoya Formation|72497|5|Briefly described|p4, p11.|Permian|Permian|After Redfern and Millward, 1994. Recognised in subsurface Barbwire Terrace area. Implied to be part equivalent of Winifred Formation.||upper Grant Group||Shown as underlying Calytrix Formation.|Includes some glaciogenic sediments such as dropstones.|
31465|Hoya Formation|73117|4|Described|p: 13, 15, 22, 24-26, 111-115, 117, 123|Asselian|Gzhelian|Name proposed by Redfern (1991) as an alternative subdivision of the Grant Group to that of Of Crowe and Towner (1975). Associated with Microbaculispora tentula Zone and P. confluens Zone. Name derived from a well at the south-eastern end of the Barbwire Terrace. This scheme for constituents of the Grant Group has been applied inconsistently across the Barbwire Terrace. Proposed lectostratotype section from Pratia 1 well (Apak and Backhouse, 1999).||Grant Group||Overlain[?] by Calytrix Formation.|Glacial facies.|
38797|Hughes Dolerite|23926|6|Mentioned|p33 Fig. 15|||Geological Province: Yilgarn Craton.||||||
38797|Hughes Dolerite|23931|6|Mentioned|p200 Fig.2|||Geological Province: Yilgarn Craton.||||||
80119|Humpback Leucogranite|71212|5|Briefly described|p3, p74, p82-p84, p114-116|Neoarchean|Neoarchean|Yilgarn Craton. See also p46, 72, 86, 87, 88, p91, p108, p110, p113-p118, p120, p146, p147, p195, p198, p228, p231, p232, p251, p252, p260, App C.|2593 Ma (Rb-Sr whole rock)||||Generally massive, medium to coarse-grained, sporadically muscovitic, leucocratic granite with no foliation.|26-SEP-17
77685|Hyland Bay Subgroup|69452|5|Briefly described|p36:8, 15, 19-20|||Hughes (1978); redefined in Gorter (1998). Petrel Sub-basin, Bonaparte Basin. Up to c.2300m thick collectively.||Kinmore Group.|Torrens, Pearce, Cape Hay, Dombey, Tern Formations.|Is overlain unconformably by Mount Goodwin Subgroup.|Mudstone, siltstone, sandstone and carbonate rocks.|12-JUL-16
77685|Hyland Bay Subgroup|69454|5|Briefly described|p38:4|Changhsingian|Sakmarian|Petrel Sub-basin, Bonaparte Basin.||Kinmore Group.|Fossil Head, Torrens, Pearce, Cape Hay, Dombey, Tern Formations.|Overlies Kulshill Group. Is overlain by Mount Goodwin Subgroup.||12-JUL-16
77685|Hyland Bay Subgroup|69673|5|Briefly described|p153 fig 125, p173|||2300m thick.||Kinmore Group|Includes Torrens Formation, Pearce Formation, Cape Hay Formation, Dombey Formation, Tern Formation||Mudstone, siltstone, sandstone and carbonate rocks.|
77685|Hyland Bay Subgroup|70061|4|Described|Petrel Sub-basin; Figs.2 & 3, p2|Changhsingian|Roadian|See also Regional geology: Figs.6-8, p8-11, p13, p15-16, p19. Vulcan: Fig.2, p2. Hydrocarbon source. Pro-delta, shoreface and open marine sediments. Sealed by thick marine shales of Mount Goodwin Subgroup and Flamingo Group. Units in this Subgroup are now considered primary exploration targets in the central Petrel Sub-basin. Potential gas reservoir in Vulcan Sub-basin. Appears as Hyland Bay Formation on p19.||Kinmore Group.|Torrens, Pearce, Cape Hay, Dombey and Tern Formations.|Overlies Fossil Head Formation. Is overlain by Mount Goodwin Subgroup.|Includes gas-prone shales.|12-JUL-16
77685|Hyland Bay Subgroup|71146|5|Briefly described|p6,  p43 fig 33|Guadalupian|Guadalupian|Bonaparte Basin.||||Overlies the Fossil Head Formation. Overlain by the Mount Goodwin Subgroup.|Mixed sandstone, mudstone, carbonate and coal.|
40767|Ida Hill Complex|24494|6|Mentioned|p19|||||||||
40767|Ida Hill Complex|63980|4|Described|pp57-59.|Archean|Archean|Kurnalpi Terrane. An intermediate-felsic volcanic centre 25 km SSE of Laverton. 3 to 5 km thick. Mainly subaqueous volcanism and reworking. The Complex was an emergent volcanic island during latter phases of volcanism.|||||Basaltic andesite and associated hyaloclastites; andesitic conglomerates, breccias and sandstone; andesite-dacite, variably porphyritic and amygdaloidal; fine-grained sedimentary rocks, chert, minor banded iron formation. Mafic to felsic intrusions.|26-SEP-14
40767|Ida Hill Complex|65264|5|Briefly described|p19|||Located on LAVERTON map sheet. Andesite and plagioclase(-hornblende) porphyritic andesite are dominant rock types.||||||07-FEB-11
40767|Ida Hill Complex|66880|5|Briefly described|p17, p29. |Archean|Archean|Kurnalpi Terrane. Large scatter and many discordant ages suggest this age may be unreliable.|c.2658 +/- 9 Ma.|||Intruded by high-Ca and mafic granite suites.|Includes quartz-feldspar porphyry.|
25955|Ilgarari Formation|22905|5|Briefly described|p52 Fig. 2, p53 Table 1|Mesoproterozoic|Mesoproterozoic|Supersedes the Kurabaka Formation (Mucalana Subgroup). Of the Collier Group.  Underlying unit: Calyie Formation.  Max. thickness: 680m.  See also p54.||||||24-JAN-06
25955|Ilgarari Formation|24115|4|Described|p4 Fig.2|Mesoproterozoic|Mesoproterozoic|Of the Collier Group. Maximum Thickness: 680m. Overlies the Calyie Formation. Geological Province: Collier Basin.||||||
25955|Ilgarari Formation|24183|2|Defined|p4 Fig.3, p20, p24|Stenian|Ectasian|Age: c.1300-1070 Ma. Geological Province: Bangemall Basin. Max. Thickness: 680m. Overlies the Calyie Formation. Equivalent of the Kurabuka Formation.||||||
25955|Ilgarari Formation|24544|4|Described|p44 Fig.32|Mesoproterozoic|Mesoproterozoic|Of Collier Group. Superseded Kurabuka Formation. Overlies Calyie Formation.||||||
25955|Ilgarari Formation|36551|6|Mentioned|p101|||||||||
25955|Ilgarari Formation|38299|5|Briefly described|p14|||||||||
25955|Ilgarari Formation|40089|2|Defined|p52|Mesoproterozoic|Mesoproterozoic|||||||
25955|Ilgarari Formation|40989|4|Described|p34|||||||||
25955|Ilgarari Formation|42013|5|Briefly described|Map legend|Proterozoic||||||||
25955|Ilgarari Formation|43238|5|Briefly described|p7|||||||||
25955|Ilgarari Formation|44142|5|Briefly described|p312, 314 Tb.4-4, p320, p322-324|||Over 650m thick shallow water suspension deposition in marine lagoons or small sub-basins below wave base. Top eroded.||Collier Subgroup||Overlies Calyie Sandstone conformably. Direct correlate of Kurabuka Formation and Balfour Formation.|Siltstone, shale, fine grained sandstone. Dolerite sills common. Basal shale manganese-enriched.|13-MAR-18
25955|Ilgarari Formation|50225|4|Described|p387 Fig. 2, p396|||Uppermost unit of Collier Group (Bangemall Supergroup). Supersedes the Kurabuka Formation. Primarily composed of parallel planar-laminated pyritic and carbonaceous siltstone. Conformably overlies Calyie Formation.  Max. thick: 700m.||||||07-FEB-11
25955|Ilgarari Formation|50226|5|Briefly described|p429|||Of the Collier Group.  Includes siltstone and sandstone which host Cu vein deposits.||||||
25955|Ilgarari Formation|60301|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Collier Group (Bangemall Supergroup). Geological Province: Collier Basin. Siltstone, mudstone, sandstone.||||||17-AUG-04
25955|Ilgarari Formation|60535|5|Briefly described|p556 Fig.1|Mesoproterozoic|Mesoproterozoic|Of the Collier Group (Bargemall Supergroup).||||||
25955|Ilgarari Formation|63866|5|Briefly described|p162-p163|||Intruded by a suite of dolerite sills which constrain the minimum age of the Collier Group.||Collier Group||||
25955|Ilgarari Formation|63869|4|Described|p39, p41, p42, Plate 1|Mesoproterozoic|Mesoproterozoic|Replaces the former Kurabuka Formation of the Mucalana Subgroup, abandoned by Cooper et al. (1998). Sedimentary units total c.680 m thickness. Ages inferred from detrital zircons and dolerite sills.|< c.1400 - c.1070 Ma.|Topmost unit in Collier Group.||Conformably overlies Calyie Formation.|Greenish-grey to black, parallel-planar laminated, pyritic and carbonaceous siltstone, locally silicified. Thin interbeds of sandstone occur in upper parts; also includes chert (silicified lutite), minor limestone and calcareous siltstone.|
25955|Ilgarari Formation|64580|6|Mentioned|map legend||Mesoproterozoic|Of Collier Group. Part of depositional package 6.||||||15-DEC-08
25955|Ilgarari Formation|64728|5|Briefly described|p95 Fig.2.|Mesoproterozoic|Mesoproterozoic|||Unit in Collier Group.||Overlies Calyie Formation.|Deep-marine mudstones; sandstone turbidites.|
25955|Ilgarari Formation|65830|4|Described|p7, p8, p9, p10-11; Plates 1,2|Stenian|Calymmian|~680m thick. Deep-marine shelf mudstone.||Of the Collier Group||Underlain by the Calyie Formation.|Consists of greenish-grey to black, parallel-planar-laminated, pyritic and carbonaceous siltstone that is locally silicified. Thin interbeds of massive to planar-laminated fine-grained sandstone are present in the upper parts of the Formation.|
25955|Ilgarari Formation|66104|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Unit in upper Collier Group. Siltstone, mudstone, and fine-grained sandstone. Includes a mapped but unnamed unit of chert and silicified siltstone.||||||19-JAN-12
25955|Ilgarari Formation|66107|5|Briefly described|p4 Fig.1|Mesoproterozoic|Mesoproterozoic|||Of the Collier Group||||
25955|Ilgarari Formation|66241|5|Briefly described|pp1-4, p9. |Mesoproterozoic|Mesoproterozoic|||Topmost unit in Collier Group.||Overlies Calyie Formation.|Deeper marine siltstone, mudstone and fine-grained sandstone.|
25955|Ilgarari Formation|67136|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin.||Unit in Collier Group.||Overlies Calyie Formation.|Siltstone, mudstone and fine-grained sandstone.|
25955|Ilgarari Formation|67374|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin.||Unit in Collier Group.|||Siltstone, mudstone and fine-grained sandstone.|
25955|Ilgarari Formation|68285|5|Briefly described|Map Legend|Stenian|Calymmian|Collier Basin.||Of the Collier Group.||Underlain by the Calyie Formation.|Siltstone, mudstone, and fine-grained sandstone.|
25955|Ilgarari Formation|68286|5|Briefly described|Map Legend|Stenian|Calymmian|Collier Basin.||Of the Collier Group||Underlain by the Calyie Formation.|Siltstone, mudstone, and fine-grained sandstone.|
25955|Ilgarari Formation|69003|5|Briefly described|p34, p53|Mesoproterozoic|Mesoproterozoic|Collier Basin, Capricorn Orogen.||Collier Group.||Overlies Calyie Formation.|Deep-marine sedimentary rocks.|
25955|Ilgarari Formation|69010|5|Briefly described|Map Legend|Stenian|Calymmian|Collier Basin. An unnamed sub-unit of chert and silicified siltstone is mapped separately.|1460-1070 Ma|Of the Collier Group.|||Comprises siltstone, mudstone, and fine-grained sandstone.|24-APR-14
25955|Ilgarari Formation|69027|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Collier Basin.||Of the Collier Group.||Underlain by the Calyie Formation.|Siltstone, mudstone, and fine-grained sandstone.|05-MAY-14
25955|Ilgarari Formation|69028|5|Briefly described|Map Legend|Stenian|Stenian|Collier Basin.||Of the Collier Group.|||Siltstone, mudstone and fine-grained sandstone.|06-MAY-14
25955|Ilgarari Formation|69091|5|Briefly described|p202|||Collier Basin. Thickness: up to 700m|||||Planar-laminated pyritic and carbonaceous siltstone and fine-grained sandstone, with minor limestone, calcareous siltstone and chert.|
25955|Ilgarari Formation|69166|4|Described|geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|||Collier Group|||Chert and silicified siltstone, mudstone and fine grained sandstone.|
25955|Ilgarari Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|||Part of Collier Group Depositional package 6.||Unit of Collier Group.||||
25955|Ilgarari Formation|69596|6|Mentioned|p12 Fig.7, p17, p30|||Collier Basin.||Collier Group.||||
25955|Ilgarari Formation|70132|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Collier Basin.||Collier Group.||Overlies Calyie Formation.|Siltstone and fine-grained sandstone; minor chert and limestone.|
25955|Ilgarari Formation|70136|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Collier Basin. The two facies associations are mapped separately.||Collier Group.|||Siltstone, mudstone and fine-grained sandstone; chert and silicified siltstone.|
25955|Ilgarari Formation|70767|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin.||Collier Group.||Overlies Calyie Formation. Is intruded by Kulkatharra Dolerite.|Siltstone and fine-grained sandstone; minor chert and limestone.|
25955|Ilgarari Formation|70768|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin.||Collier Group.||Overlies Calyie Formation. Is intruded by Kulkatharra Dolerite.|Siltstone and fine-grained sandstone; minor chert and limestone.|
25955|Ilgarari Formation|70795|5|Briefly described|100k_geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Also 100k_interpgeop_lut.csv, West Australian Craton, Collier Basin|1171-1070 Ma|Collier Group|||Siltstone and fine grained sandstone, chert and silicifed siltstone; minor limestone.|
25955|Ilgarari Formation|70814|4|Described|p5, p15-p17|||Collier Basin. Interpreted to have been deposited under deep-marine shelf conditions. This unit reaches a maximum thickness of up to 1500m. See also p20, p22, p25-p26, p28-p29, p42, p48-p49. ||Collier Group||Conformably overlies the Calyie Formation.|Planar laminated pyritic and carbonaceous siltstone with thin beds of massive to planar-laminated fine-grained sandstone and interbedded siltstone. Minor limestone, calcareous siltstone and chert also occur.|
25955|Ilgarari Formation|71042|6|Mentioned|p97|||Collier Basin. Hosts regionally extensive sheets of supergene enriched manganiferous bands within siltstones of this unit.|||||Siltstones.|
25955|Ilgarari Formation|71158|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin.||Collier Group.|||Siltstone and fine-grained sandstone; minor chert and limestone.|
25955|Ilgarari Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, mudstone, shale, sandstone|
25955|Ilgarari Formation|72259|6|Mentioned|p3|||||Collier Group||||
25955|Ilgarari Formation|72705|5|Briefly described|p3|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||Collier Group.||Overlies Calyie Formation.||
25955|Ilgarari Formation|73442|5|Briefly described|p20|||Also referred to as part of Collier Group - Depositional Packages 5 and 6.||Collier Group||Intruded by Kulkatharra Dolerite|Siltstone.|
78638|Illaara Formation|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Mesoarchean|Illaara greenstone belt, Southern Cross Domain, Youanmi Terrane|||Includes unnamed subunit.||Quartzite and quartz-rich metasedimentary rock; locally fuchsitic; includes subordinate quartz-muscovite schist and ferruginous intercalations; sandstone, with minor siltstone and pebbly sandstone; metamorphosed.|06-AUG-15
78638|Illaara Formation|69583|5|Briefly described|Plate 2|Archean|Archean||c.3000 Ma.||||Quartzite and quartz-rich metasedimentary rock, locally fuchsitic; metamorphosed sandstone with minor siltstone and pebbly sandstone.|
78638|Illaara Formation|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Mesoarchean|See also 500k_interpgeop14_lut.csv.|3131 +/- 3 Ma (isotopic) - 2700 Ma (inferred).||||Quartzite and quartz rich metasedimentary rock; locally fuchsitic; includes subordinate quartz-muscovite schist and ferruginous intercalations. Sandstone, with minor siltstone and pebbly sandstone; metamorphosed.|
78638|Illaara Formation|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma); Youanmi Terrane events (3131 - 2600 Ma). See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 100k_geologyl10_lut.csv.|3131+\-3 Ma; 2700 Ma (inferred)||||Quartzite and quartz-rich metasedimentary rock; locally fuchsitic; includes subordinate quartz-muscovite schist and ferruginous intercalations; Sandstone, with minor siltstone and pebbly sandstone; metamorphosed.|
78638|Illaara Formation|71802|5|Briefly described|p279, p286-p288|||Illaara greenstone belt and Maynard Hills greenstone belt.|||||Quartzite, conglomerate and quartz-mica schist.|
78638|Illaara Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Mesoarchean|Youanmi Terrane.|Max age 3131+/-3 Ma, min ~2700 Ma.||||Quartzite and quartz-rich metasedimentary rock; locally fuchsitic; includes subordinate quartz--muscovite schist and ferruginous intercalations.|
75776|Illgalara Monzogranite|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. Misspelt as Illigalara Monzogranite in' Parent Name' field.||Jungar Suite|Includes 1 unnamed subunit.||K-feldspar megacrystic monzogranite and equigranular granitic rock; locally laminated; metamorphosed; includes deeply weathered rock.|
75776|Illgalara Monzogranite|69583|5|Briefly described|Plate 2|Archean|Archean|||Jungar Suite.|||K-feldspar megacrystic monzogranite and equigranular granitic rock; metamorphosed.|
75776|Illgalara Monzogranite|69584|5|Briefly described|p5 Fig.2|Neoarchean|Neoarchean|||Jungar Suite|||Monzogranite.|
75776|Illgalara Monzogranite|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Jungar Suite.||||
75776|Illgalara Monzogranite|70796|5|Briefly described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton. See also 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, Madoonga100_2444_stratig.pdf.|ca 2665  2640 ma (inferred)|Jungar Suite|||Kfeldspar megacrystic monzogranite and equigranular granitic rock; locally laminated; metamorphosed. Equigranular granitic rock; metamorphosed; includes deeply weathered rock.|
75776|Illgalara Monzogranite|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv.|2665-2640 Ma|Unit of Jungar Suite.|||K-feldspar megacrystic monzogranite and equigranular granitic rock; locally laminated; metamorphosed|
75776|Illgalara Monzogranite|71271|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton.||Jungar Suite.|||Equigranular granitic rock, metamorphosed; includes deeply weathered rock.|
75776|Illgalara Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|||Jungar Suite|||K-feldspar megacrystic monzogranite and equigranular granitic rock; locally laminated; metamorphosed.|
30206|Illjarra Sandstone|22496|3|Fully described|p10||Neoproterozoic|Previously mapped as Wade Creek Sandstone. Ruby Plains Group, Wolfe Basin||||||
30206|Illjarra Sandstone|22777|5|Briefly described|Map|||Ruby Plains Group, Wolfe Basin||||||17-OCT-12
30206|Illjarra Sandstone|23314|4|Described|332|||||||||
30206|Illjarra Sandstone|23621|2|Defined|p52 Appendix|Cryogenian|Tonian|See also page 33, 9 Table 1. Type section included. Of Ruby Plains Group. Overlying unit Duerdin Group (disconformity). Underlying unit Eliot Range Dolomite (unconformity). Wolfe Basin. Max. thickness: 1000 m.||||||
30206|Illjarra Sandstone|23622|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Ruby Plains Group. Geological Province: Wolfe Basin.||||||
30206|Illjarra Sandstone|24173|4|Described|p24, p11 Tb.2|Tonian|Tonian|Of the Ruby Plains Group. Overlies the Eliot Range Dolomite (conformably/disconformably); overlain unconformably by Moonlight Valley Tillite and Ranford Formation (Duerdin Group). Geological Province: Wolfe Basin. Max Thickness: 300m.||||||06-APR-05
30206|Illjarra Sandstone|43303|5|Briefly described|Map Legend||Neoproterozoic|of Ruby Plains Group.||||||
30206|Illjarra Sandstone|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Ruby Plains Group. Geological Province: Wolfe Creek Basin. Lithic sandstone, minor siltstone and dolomite.||||||
30206|Illjarra Sandstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Cryogenian|Cryogenian|Wolfe Creek Basin||Ruby Plains Group|Includes 3 unnamed members.||Lithic sandstone; minor siltstone and dolostone; members also include shale, mudstone, dolomitic sandstone.|31-JUL-15
30206|Illjarra Sandstone|69165|4|Described|100k_interpgeop_lut.csv|Neoproterozoic|Neoproterozoic|||Ruby Plains Group|||Quartz and lithic sandstone; minor dolostone. Shale, siltstone, mudstone and sandstone.|
30206|Illjarra Sandstone|69634|4|Described|100k_interpgeop_lut.csv|Cryogenian|Cryogenian|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1.|830-810 Ma (Inferred)|Unit of Ruby Plains Group.|||Lithic quartz sandstone, dolomitic sandstone; shale, mudstone, siltstone and dolostone|
30206|Illjarra Sandstone|70154|5|Briefly described|100k_interpgeop_lut.csv|Cryogenian|Neoproterozoic||810-1000 Ma|Ruby Plains Group|||Lithic sandstone, shale, silstone and mudstone. Minor dolostone. Dolomitic sandstone.|
30206|Illjarra Sandstone|71267|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|830-720 Ma (inferred)|Unit of Ruby Plains Group.|||Lithic sandstone; shale, siltstone and dolostone, dolomitic and non-dolomitic sandstone|
77240|Ilurpa suite|66256|5|Briefly described|p8, p18 Fig.14, p24-31, see comments|Stenian|Stenian|Age: early Musgravian. In northeastern part of Tjuni Purlka Tectonic Zone. Compositionally heterogeneous throughout. Geochemistry provided. See also p34-36, p38, p41, p44, p53 App.1, p65-66 App.3|1188+/-4 Ma (SHRIMP: GSWA).|Pitjantjatjara Supersuite||||11-JAN-17
77240|Ilurpa suite|67375|6|Mentioned|p25 Fig.17, p26 Fig.19. |Mesoproterozoic|Mesoproterozoic|A-type. Yb-enriched, within-plate granite. Early Musgrave Orogeny.||Unit in Pitjantjatjara Supersuite.||||
77240|Ilurpa suite|67553|6|Mentioned|p27-28,33|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province, North Australian Craton. Early Musgravian granite.||Unit of Pitjantjatjara Supersuite.||||
77240|Ilurpa suite|69091|5|Briefly described|p64 Fig.4.10|||Early Musgravian granite.||Pitjantjatjara Supersuite|||Granite.|26-SEP-14
77240|Ilurpa suite|69729|5|Briefly described|p74 Fig.7, p77-78|||Geochemistry plots.||Pitjantjatjara Supersuite.|||A-type granites.|
75572|Ima Ima beds|65074|4|Described|p349, p351 fig 4-37, p352, p355 Tb. 4-11|Mesoproterozoic|Mesoproterozoic|Of NW Birrindudu Basin. ~1000m thick. Forms low strike ridges. Reference area 10 km NE of Wolfe Creek Meteorite Crater.||||Probably equivalent to Birrindudu Group.|Arenite and shale, conglomerate, siltstone, glauconitic and dolomitic sandstone.|
81547|Imbin Porphyry|71484|5|Briefly described|p123,125,130|Orosirian|Orosirian|Dated at 1990+\-6 Ma (Nelson, 2001). Included in Yelma Formation by Sheppard et al.( 2016). Part  of Tooloo Group.||Included in Yelma Formation?|||Felsic volcanics and felsic porphyry.|30-AUG-19
31766|Impey Granite|23569|4|Described|p5 Tb. 1|Archean|Archean|Of the Narryer Terrane.   Heterogenous coarse-grained, porphyritic to equigranular amphibolite-facies monzogranite.||||||07-NOV-08
31766|Impey Granite|23574|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Balla Granite.||||||07-NOV-08
31766|Impey Granite|23576|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Balla Granite.||||||07-NOV-08
31766|Impey Granite|23577|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Balla Granite.||||||07-NOV-08
31766|Impey Granite|24114|5|Briefly described|p5 Fig.4|||Geological Province: Yilgarn Craton.||||||
31766|Impey Granite|43835|5|Briefly described|Map Legend|Archean|Archean|||||||07-NOV-08
31766|Impey Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
31766|Impey Granite|71269|6|Mentioned|1m_geologyp12_lut.csv||||||||Heterogenous coarse-grained, porphyritic to equigranular amphibolite-facies monzogranite.|
31766|Impey Granite|73526|5|Briefly described|p2 Fig.1, p3|||Narryer Terrane, central. Undated, considered to have not been emplaced at c.2640 Ma (Myers, 1997b).|||||Multiple monzogranite intrusions.|
40281|Indee Suite|61253|5|Briefly described|p56, p52 Fig. 2, p54-55 Fig. 3|Archean|Archean|Of the Sisters Supersuite.  Collectively refers to intrusive rocks within the Mallina Basin which includes a suite of high-Mg diorite (sanukitoid) intrusions (Smithies and Champion 2000).  Age: >2.9Ga. Geological Province: Pilbara Craton/Mallina.||||||07-NOV-08
40281|Indee Suite|63441|3|Fully described|p33 Fig. 12, p37|Archean|Archean|Of Sisters Supersuite. Informally named "Pilbara high-Mg diorite suite". Includes Geemas, Jallagnoonina, Jones Well, Mallindra Well, Peawah and Wallareenya Granodiorites+ Toweranna Porphyry. All intrude De Grey Supergroup (Mallina Basin). Age: 2954-2945Ma||||||07-FEB-11
40281|Indee Suite|63538|6|Mentioned|p6 Fig. 3|Archaean|Archaean|Geological Province: Pilbara Craton.||||||19-APR-13
40281|Indee Suite|64632|6|Mentioned|p203, p205|Mesoarchean|Mesoarchean|Composition of granites influenced by subduction|2955-2945 Ma|Of the Sisters Supersuite.|||Sanukitoid.|
40281|Indee Suite|66217|5|Briefly described|p42, p43.|Mesoarchean|Mesoarchean|Mallina Basin. Hosts PGE and orthomagmatic gold deposits.|2955-2945 Ma.|Unit in Sisters Supersuite.|||Includes sanukitoids.|
40281|Indee Suite|67201|4|Described|p7 Fig.4, p22 Fig.13, p23-24|||West Pilbara Superterrane. In De Grey Superbasin.|2955-2945 Ma|Sisters Supersuite|||Sanukitoids.|
40281|Indee Suite|69185|5|Briefly described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Sisters Supersuite.|Includes Peawah Granodiorite, Toweranna Porphyry.|||
40281|Indee Suite|69301|5|Briefly described|p5 Fig.3|||Pilbara Craton. West Pilbara Superterrane.|||||Granitic rocks.|
40281|Indee Suite|69590|5|Briefly described|500k_geologyp08_lut.csv|||Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; North Pilbara Orogeny.||Unit of Sisters Supersuite.|Includes Peawah Granodiorite.|||
40281|Indee Suite|70022|6|Mentioned|p115|||West Pilbara Superterrane.||||||
40281|Indee Suite|70775|4|Described|iii, p29 tbl 5, p41|Mesoarchean|Mesoarchean|Mallina Basin. Geochronology indicates that this suite is coeval with the Portree Suite. See also p55, p64-p65, p72, p77.|c. 2950 Ma (Smithies et al 2004a)||Includes the Geemas Granodiorite, Jallagnoonina Granodiorite, Jones Well Granodiorite, Mallindra Well Granodiorite, Peawah Granodiorite, Wallareenya Granodiorite and the Toweranna Porphyry.|Intrudes the Croydon Group.|Massive to moderately foliated, mesocratic, hornblende-biotite granodiorite, sanukitoids, tonalite and hornblende-biotite granodiorite.|
40281|Indee Suite|72034|6|Mentioned|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Chillerina Granodiorite, Jallagnoonina Granodiorite, Mallindra Well Granodiorite, Peawah Granodiorite, Wallareenya Granodiorite.|||
40281|Indee Suite|72668|5|Briefly described|p4, p15-17, p22|||West Pilbara Superterrane, Mallina Basin. Geochemistry discussed.|2955-2945 Ma|Sisters Supersuite|||Sanukitoids.|
42375|Ininti Granite|61387|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Foliated porphyritic biotite granite. Age: 1688Ma.  Geological province: Arunta region.||||||07-NOV-08
42375|Ininti Granite|61519|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 1688Ma. Foliated porphyritic biotite granite; moderate magnetic intensity. Geological Province: Warumpi Province.||||||15-DEC-08
42375|Ininti Granite|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Foliated porphyritic biotite granite and granitic gneiss.||||||15-DEC-08
42375|Ininti Granite|68077|6|Mentioned|p39|||Western Arunta Orogen.||||||07-SEP-17
42375|Ininti Granite|68994|4|Described|p1, p4, p6-9, p11, p15, p23-24, p26-27|Statherian|Statherian|Warumpi Province. Part of suite of intrusive rocks formed c. 1690-1660 Ma (Meixner et al 2004; Scrimgeour et al. 2005). Sample analysed is a fine-grained, leucocratic metasyenite correlated with Ininti Granite. U-Pb zircon magmatic crystallisation age. Hf analyses provided.|1691 +/- 5 Ma (Kirkland et al. 2009).||||Felsic magmatic rocks. Syenogranitic gneiss. High-K calcalkaline granite. Variably deformed.|13-JAN-17
42375|Ininti Granite|69003|5|Briefly described|p5, p31-32|Paleoproterozoic|Paleoproterozoic|Warumpi Province, West Arunta Orogen. Part of the Argilke Event.|1691 +/- 5 Ma.|||Is overlain by Pollock Hills Formation. Is intruded by Mount Webb Granite.|Strongly foliated metasyenogranite; contains metasedimentary xenoliths.|
42375|Ininti Granite|69031|5|Briefly described|p4, p6 Fig.4, p7, p14, p17-22, p24|Statherian|Statherian|Amongst the oldest rocks in the Warumpi Province, Arunta Orogen. Emplaced during the Argilke Igneous Event. Gravity, magnetic maps. This crystallisation age is identical within error with a NT age of 1688 +/- 8 Ma (Worden et al., 2008).|1691 +/- 5 Ma (Kirkland et al., 2009).|||Intrudes Walungurru Volcanics and Pollock Hills Formation.|A strongly foliated metasyenogranite containing sedimentary xenoliths and pegmatite veins parallel to the foliation.|
42375|Ininti Granite|69417|6|Mentioned|p2:5|Statherian|Statherian|Kintore Domain, Warumpi Province.||||||12-JUL-16
42375|Ininti Granite|69428|5|Briefly described|p13:3, 12|Paleoproterozoic|Paleoproterozoic|Close et al. (in prep). Kintore Domain, Warumpi Province. Forms a number of low isolated outcrops and pavements NW of the Winnecke Hills. SHRIMP U-Pb zircon age. A syenogranite across the WA border, regarded as part of this unit, was similarly dated at 1691 +/- 5 Ma (Kirkland et al., 2009).|1688 +/- 3 Ma (Worden et al., 2006).||||A biotite porphyritic granodiorite; K-feldspar phenocrysts to 2cm, locally tabular and simply-twinned; 10% biotite that defines a well-developed foliation.|12-JUL-16
42375|Ininti Granite|69933|5|Briefly described|v, p1, p17-19, p36|Statherian|Statherian|Petrography, zircon characteristics, SHRIMP analyses and results are provided.|1688 +/- 5 Ma (SHRIMP U-Pb, magmatic age)||||Biotite porphyritic granite with K-feldspar phenocrysts and biotite defining a well developed foliation.|21-APR-23
42375|Ininti Granite|70826|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|Warumpi Province.||||||
42375|Ininti Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
42375|Ininti Granite|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1688+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Foliated biotite granite.|
42375|Ininti Granite|71810|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Warumpi Province, Arunta Orogen, North Australian Craton.|c.1691 Ma.||||Foliated, porphyritic granitic gneiss; may include syenogranitic gneiss with metasedimentary xenoliths.|
42375|Ininti Granite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Warumpi Province, Arunta Orogen.|||||Foliated, porphyritic granitic gneiss; may include syenogranitic gneiss with metasedimentary xenoliths.|
42375|Ininti Granite|72360|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological province: Warumpi Province. Of Kintore Domain. Geochron Sample No: MR01IRS85. Location: 511889E, 7429825N.|1688 Ma||||Foliated porphyritic biotite granite.|09-SEP-19
42375|Ininti Granite|73058|6|Mentioned|p777|||Arunta Orogen, west.||||||
40331|Iowa Eastern Member|24573|4|Described|p685, 689|||Of the Marillana Formation. Geological Province: central Hamersley Range. Previously part of the "Surface Weathered Zone". Contains internal subdivisions: Iowa Eastern Clay (lower) and Iowa Eastern CID (upper)||||||
40331|Iowa Eastern Member|60539|5|Briefly described|p498, 500, 501 Fig.3, 517|Miocene|Miocene|Of the Marillana Formation. Geological Province: Pilbara Craton. Thickness: ~20 m. Comprises clay and channel iron deposits. Overlies: Barimunya Member. Underlies: Oakover Formation.||||||
40331|Iowa Eastern Member|63432|5|Briefly described|p736 Fig. 3|||Uppermost member of the Marillan Formation. Overlies Weeli Wolli Formation; underlies Oakover Formation. Clay unit. See also Iowa Eastern Clay - names are used interchangeably.||||||07-FEB-11
40331|Iowa Eastern Member|65194|5|Briefly described|p107-108, p111-112|||Topmost channel iron deposit of Marillana Formation. Up to 20m thick. Consists of the Iowa Eastern Clay and the Iowa Eastern channel iron deposit.||||||
40331|Iowa Eastern Member|69538|5|Briefly described|p522 Fig.5, p535, p557 Fig.32, p583-585|Miocene|Miocene|Channel iron deposits. Appears as Iowa Eastern Clay in Fig.32.||Unit in Marillana Formation.||||
27166|Irwin River Coal Measures|12733|6|Mentioned|p565.|Early Permian|Early Permian|Perth Basin. Gas-prone.||||||
27166|Irwin River Coal Measures|12758|5|Briefly described|p8 Fig. 9|Permian|Permian|Geological Province: Northern Perth Basin.||||||
27166|Irwin River Coal Measures|14227|5|Briefly described|p6, p7|Early Permian|Early Permian|Thickness: ~1700m. Geological province: Perth Basin. Delta-top deposits. Contains gas prone source rocks. See also Enclosure 2.||||||07-FEB-11
27166|Irwin River Coal Measures|14228|6|Mentioned|p5 fig 2|Early Permian|Early Permian|||||Overlain by Carynginia Formation.||
27166|Irwin River Coal Measures|15881|6|Mentioned|p62 Fig. 1|Permian|Permian|||||||12-FEB-09
27166|Irwin River Coal Measures|22814|5|Briefly described|fig2|Permian|Permian|||||||
27166|Irwin River Coal Measures|22820|5|Briefly described|p10 Fig.4|Late Permian|Early Permian|Correlates with Rosabrook C.M. Geological province: northern Perth Basin.||||||12-AUG-08
27166|Irwin River Coal Measures|23172|4|Described|Map Legend|Permian|Permian|||||||
27166|Irwin River Coal Measures|23174|3|Fully described|4,6,Fig5p8,12|Early Permian|Early Permian|||||||
27166|Irwin River Coal Measures|23279|4|Described|p13-5||Artinskian|(Clarke et al., 1951).||||||
27166|Irwin River Coal Measures|23520|5|Briefly described|p6 Fig. 4|Early Permian|Early Permian|Geological Province: Abrolhos Sub-basin.  See also p16.||||||
27166|Irwin River Coal Measures|23761|5|Briefly described|p11|||||||||
27166|Irwin River Coal Measures|23762|5|Briefly described|Map Legend|Paleozoic|Paleozoic|||||||23-DEC-09
27166|Irwin River Coal Measures|23816|4|Described|p233|Artinskian|Artinskian|Geological Province: Perth Basin. Underlying unit: High Cliff Sandstone (conformable). Overlying unit: Carynginia Formation (conformable). Max. thickness: 123 m.||||||
27166|Irwin River Coal Measures|24058|5|Briefly described|p111|Permian|Permian|Geological Basin: Perth Basin.||||||
27166|Irwin River Coal Measures|24160|6|Mentioned|p94|||Northern Perth Basin.||||||
27166|Irwin River Coal Measures|24390|5|Briefly described|p14, p15 Fig. 8|Permian|Permian|Geological Province: Perth Basin.||||||
27166|Irwin River Coal Measures|24443|5|Briefly described|Fig.30|Early Permian|Early Permian|Conformably overlies High Cliff Sandstone, unconformably overlies Precambrian basement. Overlain conformably by Carynginia Formation. Geological Province: Bight Basin.||||||03-FEB-05
27166|Irwin River Coal Measures|29548|6|Mentioned|p230|||||||||
27166|Irwin River Coal Measures|29721|6|Mentioned|Table 226|||||||||
27166|Irwin River Coal Measures|29790|6|Mentioned|p91|||||||||
27166|Irwin River Coal Measures|30263|6|Mentioned|Table 5|||Formation well bottomed in||||||
27166|Irwin River Coal Measures|30545|6|Mentioned|Fig.2|||Artinskian||||||
27166|Irwin River Coal Measures|30948|6|Mentioned|Map legend|Artinskian|Artinskian|||||||
27166|Irwin River Coal Measures|30973|6|Mentioned|Map legend|Artinskian|Artinskian|||||||
27166|Irwin River Coal Measures|31394|6|Mentioned|p60|||See also P61,62. L.Permian||||||
27166|Irwin River Coal Measures|31561|6|Mentioned|p18|||See also map P20.||||||
27166|Irwin River Coal Measures|31562|6|Mentioned|p10|||Stratigraphic Table||||||
27166|Irwin River Coal Measures|31568|5|Briefly described|p19|||L. Permian||||||
27166|Irwin River Coal Measures|31910|4|Described|Table 1|||p17.||||||18-MAR-20
27166|Irwin River Coal Measures|32113|6|Mentioned|p52|||||||||
27166|Irwin River Coal Measures|32163|6|Mentioned|p279|||Stratigraphic column Fig.2||||||
27166|Irwin River Coal Measures|32165|6|Mentioned|p196|||Sections correlated BMR10 & 10A||||||
27166|Irwin River Coal Measures|32337|4|Described|p25|||||||||
27166|Irwin River Coal Measures|32641|6|Mentioned|p5|||L.Perm.||||||
27166|Irwin River Coal Measures|32648|6|Mentioned|p32|||L. Perm.||||||
27166|Irwin River Coal Measures|32649|4|Described|p23|||See also Table 1.||||||
27166|Irwin River Coal Measures|32714|6|Mentioned|Fig.2|||||||||
27166|Irwin River Coal Measures|32835|6|Mentioned|p5|||Flora||||||
27166|Irwin River Coal Measures|32840|6|Mentioned|Table 1|||||||||
27166|Irwin River Coal Measures|33022|6|Mentioned|p261|||Palaeomagnetic results||||||
27166|Irwin River Coal Measures|33052|6|Mentioned|Fig.1|||Artinskian||||||
27166|Irwin River Coal Measures|33386|6|Mentioned|Fig.7|||||||||
27166|Irwin River Coal Measures|33701|6|Mentioned|Fig.1|||Artinskian||||||
27166|Irwin River Coal Measures|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
27166|Irwin River Coal Measures|34274|6|Mentioned|Fig.2|||Perm.See also P118||||||
27166|Irwin River Coal Measures|34532|6|Mentioned|Fig.2|||||||||
27166|Irwin River Coal Measures|34841|6|Mentioned|p95|||||||||
27166|Irwin River Coal Measures|35268|6|Mentioned|p21|||||||||
27166|Irwin River Coal Measures|35282|6|Mentioned|Fig.2|||||||||
27166|Irwin River Coal Measures|35653|6|Mentioned|p1093|||Discussion of stratigraphy and basin development. See also Fig.3.||||||
27166|Irwin River Coal Measures|35983|6|Mentioned|Table 26|||||||||
27166|Irwin River Coal Measures|36100|6|Mentioned|Fig.2|||||||||
27166|Irwin River Coal Measures|36257|6|Mentioned|Table 2.1|||||||||
27166|Irwin River Coal Measures|36265|5|Briefly described|Fig.3.26|Early Permian|Early Permian|Geological province: Perth Basin.||||||04-MAR-08
27166|Irwin River Coal Measures|36293|2|Defined|p100|Artinskian|Artinskian|||||||
27166|Irwin River Coal Measures|36890|3|Fully described|p233|||||||||
27166|Irwin River Coal Measures|36899|6|Mentioned|Fig.3|||||||||
27166|Irwin River Coal Measures|36911|6|Mentioned|p57|||||||||
27166|Irwin River Coal Measures|37065|6|Mentioned|p29|||||||||
27166|Irwin River Coal Measures|37095|6|Mentioned|p246|||||||||
27166|Irwin River Coal Measures|37104|4|Described|p271|||||||||
27166|Irwin River Coal Measures|37286|6|Mentioned|p30|||||||||
27166|Irwin River Coal Measures|37298|6|Mentioned|p91|||See also Fig.1.||||||
27166|Irwin River Coal Measures|37577|6|Mentioned|p77|||||||||
27166|Irwin River Coal Measures|37812|6|Mentioned|p653|||||||||
27166|Irwin River Coal Measures|38352|6|Mentioned|p61|||||||||
27166|Irwin River Coal Measures|38484|6|Mentioned|p6|||||||||
27166|Irwin River Coal Measures|38486|6|Mentioned|p6|||||||||
27166|Irwin River Coal Measures|38655|6|Mentioned|p6|||||||||
27166|Irwin River Coal Measures|38998|6|Mentioned|p37|||||||||
27166|Irwin River Coal Measures|39266|6|Mentioned|p222|||||||||
27166|Irwin River Coal Measures|39854|6|Mentioned|p21|||||||||
27166|Irwin River Coal Measures|40306|6|Mentioned|p59|||||||||
27166|Irwin River Coal Measures|40340|6|Mentioned|p22|||||||||
27166|Irwin River Coal Measures|40346|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
27166|Irwin River Coal Measures|40347|6|Mentioned|p25|||||||||
27166|Irwin River Coal Measures|40794|5|Briefly described|p94|||||||||
27166|Irwin River Coal Measures|40992|6|Mentioned|p6|||||||||
27166|Irwin River Coal Measures|41172|4|Described|p121|||||||||
27166|Irwin River Coal Measures|41192|6|Mentioned|Fig.5|||||||||
27166|Irwin River Coal Measures|41195|6|Mentioned|p321|||||||||
27166|Irwin River Coal Measures|41589|5|Briefly described|p118|||||||||
27166|Irwin River Coal Measures|41728|5|Briefly described|p442|||||||||
27166|Irwin River Coal Measures|41729|6|Mentioned|p453|||||||||
27166|Irwin River Coal Measures|42075|5|Briefly described|Fig.7 p247|||||||||05-MAR-08
27166|Irwin River Coal Measures|42183|6|Mentioned|p357|||||||||
27166|Irwin River Coal Measures|42309|6|Mentioned|p256|||||||||
27166|Irwin River Coal Measures|42641|6|Mentioned|p124|||Perth Basin?||||||
27166|Irwin River Coal Measures|42711|6|Mentioned|p24|||Geological province: northern Perth Basin. Equivalent to Ewington C.M. of the Collie Group in the Collie Basin.||||||
27166|Irwin River Coal Measures|43015|5|Briefly described|Table 1,p319|||||||||
27166|Irwin River Coal Measures|43018|5|Briefly described|Table 1,p386|||actually spelt Irwin R. CM||||||
27166|Irwin River Coal Measures|43031|4|Described|p12,Fig.2.|||||||||
27166|Irwin River Coal Measures|43067|5|Briefly described|p120,Fig.12,p124|||||||||
27166|Irwin River Coal Measures|43216|5|Briefly described|Map Legend||Permian|Perth Basin||||||
27166|Irwin River Coal Measures|43217|5|Briefly described|Map Legend||Permian|Perth Basin||||||
27166|Irwin River Coal Measures|43297|4|Described|p4, fig.3 p5||Artinskian|Type section location given. Also Table1 p7.||||||
27166|Irwin River Coal Measures|43347|6|Mentioned|13|||||||||
27166|Irwin River Coal Measures|43495|4|Described|6-32||Artinskian|||||||
27166|Irwin River Coal Measures|43504|4|Described|4-18||Artinskian|||||||
27166|Irwin River Coal Measures|44064|14|Not recorded|p55|||||||||
27166|Irwin River Coal Measures|44144|4|Described|p507 Tb.4-21, p509 Fig.4-145, p510|Artinskian|Artinskian|See also p511 Fig.4-147. Type Section: Irwin River North Branch; 28o56'40''S 115o32'45''E. 250m thick fluvial deposits.||||Conformably overlies High Cliff Sandstone. Overlain conformably by Carynginia Formation.|Interbedded very coarse- to very fine-grained sandstone, with claystone, siltstone, shale (often carbonaceous) and coal.|
27166|Irwin River Coal Measures|44219|14|Not recorded|p31||Artinskian|||||||
27166|Irwin River Coal Measures|44657|14|Not recorded|p.9|||||||||
27166|Irwin River Coal Measures|44994|6|Mentioned|Fig.7|||Permian.||||||
27166|Irwin River Coal Measures|45001|14|Not recorded|p146|||||||||
27166|Irwin River Coal Measures|45016|14|Not recorded|p.115,119|||Correlates with One Gum & Keogh Formations.||||||
27166|Irwin River Coal Measures|46849|6|Mentioned|p178|||||||||
27166|Irwin River Coal Measures|48614|14|Not recorded|p43,46,48 Pl.8|||||||||
27166|Irwin River Coal Measures|48615|4|Described|p.1,4,5,6,11,13,14.|||On many pages. Fig.1,3. Pl.1.  (H50-1,9).||||||
27166|Irwin River Coal Measures|48857|2|Defined|p.15-18||Permian|p.11.||||||
27166|Irwin River Coal Measures|49644|5|Briefly described|Table|||||||||
27166|Irwin River Coal Measures|49942|5|Briefly described|p4 Fig.3|Early Permian|Early Permian|Conformably overlain by Carynginia Formation. Geological Province: Gascoyne Platform.||||||
27166|Irwin River Coal Measures|50085|5|Briefly described|p15 Fig. 8|Permian|Permian|Geological Province: Northern Perth Basin.||||||11-MAY-04
27166|Irwin River Coal Measures|50107|5|Briefly described|Map legend|Permian|Permian|Geological Province: Northern Perth Basin.||||||
27166|Irwin River Coal Measures|60118|5|Briefly described|p29|Permian|Permian|Source of gas reservoir. Geological Province: Perth Basin.||||||30-MAY-06
27166|Irwin River Coal Measures|60120|5|Briefly described|p36|Early Permian|Early Permian|Geological Province: northern Perth Basin.||||||22-JUL-04
27166|Irwin River Coal Measures|60376|4|Described|p13, p38-39, p17 Fig. 4.|Early Permian|Early Permian|Geological Province: Perth Basin. Overlain by Caryinginia Formation. Underlain by High Cliff SST.||||||07-FEB-11
27166|Irwin River Coal Measures|60377|4|Described|p61 Fig. 3, p64, p72|Artinskian|Artinskian|Overlain by Carynginia Fm. Underlain by High Cliff SST. Geol Prov: Perth Basin. Depositional environment is fluvial coal swamp. Consists of sandstone with subordinate carbonaceous siltstones and shales. Coal seams are thin and discontinuous.||||||07-FEB-11
27166|Irwin River Coal Measures|60384|6|Mentioned|p243 Fig 2a|Early Permian|Early Permian|Southern Carnarvon Basin.||||||
27166|Irwin River Coal Measures|60386|5|Briefly described|p297, 311|Artinskian|Artinskian|Northern Perth Basin. Non-marine. ||||||
27166|Irwin River Coal Measures|61023|5|Briefly described|p20 Fig 10|Permian|Permian|Main prospective source for gas. Geological Province: Perth Basin.||||||11-APR-08
27166|Irwin River Coal Measures|61546|5|Briefly described|p381, p382, p385 Fig.5, p386, p392.  |Permian|Permian|Perth Basin. The primary reservoir of the commercially viable Cliff Head oil field. Sediments deposited in a fluvial to coastal plain to coal swamp environment. Late Early Permian uplift and erosion removed 400-450 m of section. Has fault planes sub-parallel to bedding planes.||||Overlies High Cliff Sandstone. Is overlain by Carynginia Formation.|A sequence of interbedded sandstones (up to 20m thick), siltstones, shales and coal.|
27166|Irwin River Coal Measures|61811|4|Described|p3 Fig.2, p36, pp38-45, p64.|Artinskian|Artinskian|Northern Perth Basin. Fluvio-deltaic facies. 66 m thick at type section (exposed on south side of Irwin River, upstream from High Cliff and Fossil Cliff); 288 m thick west of the Urella Fault. Similarly, depth of burial varies from 500-1000 m east of the fault, to c. 3500 m on the west. Type section details in Appendix 1. From 4 to 9 main seams; resource estimation hindered by facies changes, seam splits, high ash and sulfur contents.||||Overlies High Cliff Sandstone. Is overlain conformably by Carynginia Formation and, unconformably, by Victoria Plateau Sandstone.|A mixed succession of sandstone, siltstone, carbonaceous shale, and coal.|
27166|Irwin River Coal Measures|62113|4|Described|pp618-621, pp626-630.    |Artinskian|Artinskian|55-300m thick alluvial-deltaic facies deposits; brackish to freshwater setting. Flora mainly ferns and lycopods. Broadly equivalent to the Ewington Coal Measures and the lower coarse-grained sandstone of the Wooramel Group. Has potential as hydrocarbon source rocks.||||Conformably overlies the High Cliff Sandstone. Is overlain by the Carynginia Formation.|Sandstone-mudstone-coal association: low rank sub-bituminous coal is present as several discontinuous lenses up to several metres thick; laminated and rippled sandstone, laminated carbonaceous mudstone; rare conglomerate.|
27166|Irwin River Coal Measures|64580|4|Described|map legend||Early Permian|Interbedded very coarse- to fine-grained sandstone, claystone, siltstone, shale (commonly carbonaceous), and coal.||||||09-DEC-08
27166|Irwin River Coal Measures|64630|5|Briefly described|p31 Fig.2|Artinskian|Artinskian|Province: Northern Perth Basin. Underlies the Carynginia Formation, overlies the High Cliff Sandstone. Palynology age: D. byroensis to M. trisina.||||||24-NOV-09
27166|Irwin River Coal Measures|64635|5|Briefly described|p4 Fig.3, p18-26      |Artinskian|Artinskian|Of Clarke et al. (1951). Fluvial-deltaic facies. ~66m thick in the type section. Palynological studies suggest an Artinskian age (Balme in McWhae et al., 1958; Segroves, 1971). Type section diagram p20 Fig.17.||||Conformably overlies the High Cliff Sandstone. Overlain conformably by the Carynginia Formation.|Mixed succession of sandstone, siltstone, carbonaceous shale, and coal. Fossiliferous.|
27166|Irwin River Coal Measures|64972|6|Mentioned|p617 Fig. 5|Early Permian|Early Permian|Geological Province: Perth Basin.||||||
27166|Irwin River Coal Measures|64974|6|Mentioned|p144 Fig. 3|Artinskian|Artinskian|Geological Province: Perth Basin.||||||24-JUN-09
27166|Irwin River Coal Measures|64980|5|Briefly described|pp625-634.|Permian|Permian|Perth Basin. Hydrocarbon reservoir and gas source.||||Is overlain by Carynginia Formation.|Thickly interbedded interval of sandstone, siltstone, shale and minor coal.|
27166|Irwin River Coal Measures|67135|5|Briefly described|p5 Fig.7.|Permian|Permian|Perth Basin. Shown on Fig.7 as Irwin River/Sue Coal Measures.||||Overlies High Cliff Sandstone. Is overlain by Carynginia Formation.|Shale, sandstone.|
27166|Irwin River Coal Measures|67340|6|Mentioned|p6, 8, 25|Permian|Permian|Northern Perth Basin. Thermal rock properties.||||||
27166|Irwin River Coal Measures|67925|5|Briefly described|Ch3 p15, Ch4 p8 fig 2|Lower Permian|Lower Permian|Northern and central Perth Basin. ||||Overlies the High Cliff Sandstone. Overlain by the Carynginia Formation.||
27166|Irwin River Coal Measures|69029|6|Mentioned|p332|Artinskian|Artinskian|Of Perth Basin.||||Overlain by Ashbrook Sandstone. Underlain by Rosabrook Coal Measures.||
27166|Irwin River Coal Measures|69081|6|Mentioned|p735|Permian|Permian|Oil and gas produced. Age: Early Permian. Geol. Prov: Perth Basin.||||||23-JUL-15
27166|Irwin River Coal Measures|69182|5|Briefly described|Ch2 p3, Ch2 p9|Early Permian|Early Permian|Perth Basin. Age equivalent of the Rosabrook Coal Measures. Contains oil and gas. Fair to good porosity that is generally greater than 10 percent. See also  Ch2 p11, Ch2 p34-p42, Ch2 p44-p49, Ch2 p54-p55, Ch2 p57, Ch2 p60, Ch2 p64-p67, Ch2 p70-p73, Ch2 p80, Ch2 p83-p84, Ch2 p88-p91, Ch2 p92-p96, Ch2 p98-p102, Ch2 p104, Ch2 p106, Ch2 p108, Ch2 p110.||||Overlies the High Cliff Sandstone. Overlain by the Carynginia Formation.|Sandstone interbedded with siltstone and minor thin-bedded coals.|
27166|Irwin River Coal Measures|69297|6|Mentioned|p206, p237|Permian|Permian|Perth Basin. ||||||
27166|Irwin River Coal Measures|69547|6|Mentioned|p182,193,197|Artinskian|Artinskian|northern Perth Basin.||||Underlain by High Cliff Sandstone.||
27166|Irwin River Coal Measures|69583|5|Briefly described|p130, Plate 3.|Paleozoic|Paleozoic|Perth Basin.|||||Interbedded very coarse- to fine-grained sandstone, claystone, siltstone, shale (commonly carbonaceous) and coal.|
27166|Irwin River Coal Measures|70097|5|Briefly described|p2, p6, p8, p10, p20 Fig.4|Artinskian|Artinskian|Northern Perth Basin. Irwin Terrace, Greenough/Bookara Shelf, Dongara Saddle and Dandaragan Trough.||||Overlies High Cliff Sandstone. Is overlain by Kockatea Shale or Carynginia Formation.|Deltaic sediments basin fill. Includes coal.|12-SEP-17
27166|Irwin River Coal Measures|70128|5|Briefly described|p449|Permian|Permian|Northern Perth Basin.||||Conformably overlies High Cliff Sandstone. Is overlain conformably by Carynginia Formation.||
27166|Irwin River Coal Measures|70774|5|Briefly described|p5 fig 3|Artinskian|Artinskian|Northern Perth Basin.||||Overlies the High Cliff Sandstone. Overlain by the Carynginia Formation.||
27166|Irwin River Coal Measures|70796|5|Briefly described|500k_interpgeop14_lut.csv|Artinskian|Artinskian|Perth Basin. Formed during Gondwana breakup along the western margin.|290.1  283.5 Ma (biostrat)||||Interbedded very coarse to fine grained sandstone, claystone, siltstone, shale (commonly carbonaceous), and coal|
27166|Irwin River Coal Measures|70826|6|Mentioned|p6 tbl 3|Permian|Permian|Perth Basin.||||||
27166|Irwin River Coal Measures|71146|5|Briefly described|p6, p39-p40,  p43 fig 33|Artinskian|Artinskian|Perth Basin.||||Overlies the High C liff Sandstone. Overlain by the Carynginia Formation.|Mixed sandstone, mudstone and coal.|
27166|Irwin River Coal Measures|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, conglomerate, siltstone, claystone|
27166|Irwin River Coal Measures|71269|4|Described|GEOL_LUT_CSV files|Artinskian|Artinskian|Of Perth Basin. Events: Mid-Miocene transgression, 15 Ma (15-15 Ma); Wilson Bluff transgression, 42 Ma (42-42 Ma); Kings Park transgression, 56 Ma (56-56 Ma); Gondwana breakup-western margin (210-125 Ma); Jurassic-Early Cretaceous rifting, Perth Basin (168-133 Ma);??. See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv.|290.1-283.5 Ma (biostrat)||||Interbedded very coarse to fine grained sandstone, claystone, siltstone, shale (commonly carbonaceous), and coal|
27166|Irwin River Coal Measures|71623|6|Mentioned|p349 Fig 7|||||||||
27166|Irwin River Coal Measures|72034|5|Briefly described|500k_interpgeop16_lut|Artinskian|Artinskian|Perth Basin.  Age from biostratigraphy.||Permian package 1, Perth Basin.|||Interbedded very coarse to fine grained sandstone, claystone, siltstone, shale (commonly carbonaceous), and coal.|
27166|Irwin River Coal Measures|72258|5|Briefly described|p129,133-134|Cisuralian|Cisuralian|Of Perth Basin. Major peak in Mesoproterozoic (1300-1100 Ma) detrital zircons correlate with characteristic ages and Hf isotopic signatures of magmatism in the Albany-Fraser-Wilkes Orogen (Clark et al., 2000; Fitzsimons, 2000, 2003; Kirkland et al., 2011; Spaggiari et al., 2015). Late Meso- to Early Neoproterozoic (1100-900 Ma) detrital zircons atributed to Pinjarra Orogen. Bimodal Neoproterozoic 750 and 500 Ma peaks in detrital zircon ages also likely to be derived locally from Pinjarra Orogen (p134-135 describes potential, but unlikely Gondwanan sources).||||Overlain by Carynginia Formation. Underlain by High Cliff Sandstone. Laterally grades into Ashbrook Sandstone.||
27166|Irwin River Coal Measures|72505|5|Briefly described|p890|Artinskian|Artinskian|Perth Basin. Correlated with the Microbaculispora trisina zone. Includes possible thin tuff beds.||||Overlies the High Cliff Sandstone. Overlain by the Carynginia Formation.|Coal measures with possible tuffaceous layers.|18-MAR-20
27166|Irwin River Coal Measures|72910|6|Mentioned|p4 Fig.3.|Artinskian|Artinskian|Shown as part of the Northern Perth Basin.||||Overlies High Cliff Sandstone and underlies Carynginia Formation. Laterally equivalent to Woormel Group and Callytharra Formation.|Includes coal.|
27166|Irwin River Coal Measures|73184|6|Mentioned|p198|Artinskian|Artinskian|Perth Basin. Contains significant Archean zircons in places close to the Yilgarn Craton.||||||
27166|Irwin River Coal Measures|73484|5|Briefly described|p476 Fig.3|Cisuralian|Cisuralian|Perth Basin. Marine-deltaic.||||Overlies High Cliff Sandstone, underlies Carynginia Formation||
27166|Irwin River Coal Measures|73513|4|Described|p30 Fig.2, p31-35, p36 Fig.9, p39-41|Artinskian|Artinskian|Perth Basin. Coastal or lower delta plain depositional environment. About 250 m thick in the Waitsia area.||||Overlies High Cliff Sandstone with a transitional boundary, underlies Carynginia Formation|Fluvial unit. Interbedded argillaceous sandstone, siltstone, shale and thin coal.|
27166|Irwin River Coal Measures|73623|5|Briefly described|p4|Cisuralian|Cisuralian|Irwin Basin.||||Overlies High Cliff Sandstone. Is overlain by Carynginia Formation. Correlative of Wooramel Group.||
80016|Irwin River Sequence|69297|6|Mentioned|p204, p205, p223, p236|Artinskian|Artinskian|Offshore Perth Basin - Abrolhos Sub-Basin, Beagle Ridge. Displays good TOC and is a potential gas source rock.||||Overlies the High Cliff Sequence. Overlain by the Carynginia Sequence.||20-SEP-17
36833|Isabella Member|23570|4|Described|p157|Archean|Archean|See also p234 App. 1.  Of Jeerinah Formation.   Max. thickness: 50m.   Geological Province: Pilbara Craton||||||07-NOV-08
36833|Isabella Member|23575|5|Briefly described|Map Legend|Archean|Archean|Of Jeerinah Formation. Overlying unit Nallanaring Member. Underlying unit Woodiana Member. Geological Province: Hamersley Basin.||||||07-NOV-08
36833|Isabella Member|23583|5|Briefly described|Map Legend|Archean|Archean|Of Jeerinah Formation. Underlying unit Baramine Volcanic Member. Geological Province: Hamersley Basin.||||||07-NOV-08
36833|Isabella Member|23585|4|Described|p18|Archean|Archean|Of Jerrinah Formation. Underlying unit Baramine Volcanic Member. Geological Province: Hamersley Basin. Max. thickness: 200 m.||||||07-NOV-08
36833|Isabella Member|23745|4|Described|p13|Archean|Archean|See also page 7 Fig 5. Of Jeerinah Formation.||||||07-NOV-08
36833|Isabella Member|24353|5|Briefly described|p6|Archean|Archean|Parent: Barramine Volcanic Member. Geological Province: Pilbara Craton||||||07-NOV-08
36833|Isabella Member|50544|4|Described|p51, p44 Fig. 8|Archean|Archean|Lensoid unit within the Jeerinah Formation.  Fine-grained or porphyritic rhyolite.  Overlies the Baramine Volcanic Member.  Max. thick:~200m.  Geological Province: Hamersley Basin.  See also p43.||||||07-NOV-08
36833|Isabella Member|50555|5|Briefly described|Map legend|Archean|Archean|Of the Jeerinah Formation (Hamersley Group, Mount Bruce Supergroup).  Fine-grained, massive rhyolite; quartz or carbonate amygdales.  Geological Province: Hamersley Basin.||||||07-NOV-08
36833|Isabella Member|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Jeerinah Formation|||Fine-grained, massive rhyolite; quartz or carbonate amygdales; possible intrusion|
36833|Isabella Member|69590|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Of Northeast Pilbara Sub-basin, Fortescue Basin. Events: Pilbara Craton breakup. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|2715-2629 Ma (inferred)|Unit of Jeerinah Formation.|||Fine-grained, massive rhyolite; quartz or carbonate amygdales; possible intrusion|
39351|Isolated Hill Granodiorite|24091|4|Described|p100|Archean|Archean|Age: 2681+/-4Ma (Pb/Pb). Geological Province: Yilgarn Craton.||||||07-NOV-08
38636|Jack Hills metaconglomerate|23785|5|Briefly described|p19|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
38636|Jack Hills metaconglomerate|24448|5|Briefly described|p158|Archean|Archean|Age: >4000Ma and 3380+/-20Ma.  Geological Province: Yilgarn Craton.||||||07-NOV-08
38636|Jack Hills metaconglomerate|62842|6|Mentioned|p213|||Contains about 12% of old zircon population - age >3900Ma.||||||08-NOV-06
38636|Jack Hills metaconglomerate|71349|6|Mentioned|p723|||Yilgarn Craton. Contains Archean and Hadean detrital zircons.||||||
78639|Jacko Monzogranite|69152|6|Mentioned|geochron file 104975.1.pdf|||Mentioned in geochron file 104975.1.pdf (1997?) as of Mulgabbie Pluton.||||||06-AUG-15
81587|Jaguar Dolerite|72057|5|Briefly described|p238-239,243,245-248|Neoarchean|Neoarchean|Geological province: Kurnalpi Terrane, Yilgarn Craton. Thickness: 65-120m. Hosted in a succession of bimodal felsic-mafic volcanic rocks associated with the Jaguar-Bentley-Teutonic Bore VMS complex (Hallberg and Thompson, 1985; Belford, 2010; Belford et al., 2015). SHRIMP zircon age of dacite from the volcanic complex is 2692+\-4 Ma (Nelson, 1995). Interpreted as a localised mafic intrusion or ponded lava.|||||Basalt grading up to dolerite, minor gabbro, aphyric basalt.|07-FEB-20
68514|Jallagnoonina Granodiorite|63372|4|Described|Map Legend|Archean|Archean|Geological Province: Mallina Basin and east Pilbara. Tonalite and Granodiorite; metamorphosed.||||||07-NOV-08
68514|Jallagnoonina Granodiorite|63441|5|Briefly described|p11 Tb. 2, p37|Archean|Archean|Of Indee Suite (Sisters Supersuite). Geological province: Pilbara Craton.  Intrudes De Grey Supergroup.||||||07-FEB-11
68514|Jallagnoonina Granodiorite|70775|6|Mentioned|p65|||||Indee Suite||||
68514|Jallagnoonina Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite, tonaltie|
68514|Jallagnoonina Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Indee Suite|||Hornblende-biotite granodiorite; medium- to coarse-grained; metamorphosed.|
28620|James Formation|40089|6|Mentioned|p176|||||||||
75710|Jansz Sandstone|67970|5|Briefly described|p3, p13, p25 Fig.4.|Oxfordian|Oxfordian|Eastern Exmouth Plateau. Sandy shelfal facies. Reservoir in the supergiant Io/Jansz gas field. Hydrocarbon shows in Glencoe 1, Jansz 1 and Jansz 3 wells.||||Is overlain by Dingo Claystone.||
75710|Jansz Sandstone|68135|6|Mentioned|p51 fig 2a|Late Jurassic|Late Jurassic|[Mis-spelling of Jansz: appears as Janz]. Northern Carnarvon Basin.||||||14-SEP-17
75710|Jansz Sandstone|70066|5|Briefly described|Exmouth: Fig.2; p1-2. Regional: Fig.6;p6|Kimmeridgian|Oxfordian|Exmouth Plateau, Northern Carnarvon Basin. Significant petroleum reservoir: hosts the giant Io/Jansz gas accumulation.||||Overlies Athol Formation. Is overlain by Dingo Claystone.||
25961|Jarlemai Siltstone|7433|5|Briefly described|p25 Fig.2, pp42-44, p53.|Early Cretaceous|Jurassic|Canning Basin. Shallow marine mudstone. Maximum thickness 259 m. |||Contains a nodular phosphate bed informally known as "Langey Shale" in pre-1970s literature.|Overlies Alexander Formation. Is overlain by several units, including Broome Sandstone, Mowla Sandstone, Callawa Formation and probably Frezier Sandstone.|Massive sandy mudstone; extensively bioturbated. Glauconitic in subsurface. Contains phosphatic ironstones, and a basal nodular phosphate bed 40 km SSW of Derby.|
25961|Jarlemai Siltstone|22717|5|Briefly described|P11, P12|Cretaceous|Jurassic|||||||
25961|Jarlemai Siltstone|22718|5|Briefly described|P8, Table1 P6|Tithonian|Oxfordian|||||||
25961|Jarlemai Siltstone|22738|4|Described|10,13,14,16, map|Early Cretaceous|Late Jurassic|Max thickness 200 m. Overlain by Broome Sandstone, Callawa Formation; underlain by Alexander Formation.||||||13-NOV-07
25961|Jarlemai Siltstone|22753|5|Briefly described|Fig.3 p585|Jurassic|Jurassic|||||||
25961|Jarlemai Siltstone|22765|5|Briefly described|P10|Tithonian|Oxfordian|Underlain by Alexander Formation.||||||13-NOV-07
25961|Jarlemai Siltstone|22767|5|Briefly described|Table3 P12, P23|Cretaceous|Oxfordian|||||||
25961|Jarlemai Siltstone|22776|4|Described|p21,Table.3|Tithonian|Middle Oxfordian|Min age Early Tithonian.||||||
25961|Jarlemai Siltstone|22814|5|Briefly described|fig2|Jurassic|Jurassic|||||||
25961|Jarlemai Siltstone|23212|4|Described|Table.1 p11|Tithonian|Kimmeridgian|Age: May extend to Early Cretaceous.||||||
25961|Jarlemai Siltstone|23575|5|Briefly described|Map Legend|Mesozoic|Mesozoic|||||||
25961|Jarlemai Siltstone|23722|6|Mentioned|p35|||||||||
25961|Jarlemai Siltstone|23757|4|Described|p16|Jurassic|Jurassic|Disconformably overlies Wallal Sandstone; disconformably overlapped by Callawa Fm. Max. thickness: 74m. Geological Province: Westralian Superbasin. Comprises light grey to black silty mudstone and minor thin beds of fine-grained sandstone and siltstone.||||||07-JAN-08
25961|Jarlemai Siltstone|23765|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||
25961|Jarlemai Siltstone|23766|4|Described|p13 Tb. 2|Late Jurassic|Early Jurassic|Consists of siltstone and minor limestone. Thickness: 238m. See also p28.||||||01-JUL-08
25961|Jarlemai Siltstone|24061|5|Briefly described|p183|Jurassic|Jurassic|Geological Province:  Canning Basin.||||||
25961|Jarlemai Siltstone|24062|5|Briefly described|p186 Table 1|Cretaceous|Jurassic|Geological Province: Canning Basin.||||||
25961|Jarlemai Siltstone|30021|6|Mentioned|p97|||||||||
25961|Jarlemai Siltstone|30110|6|Mentioned|p81|||See also p84. Kimmeridgian age.||||||13-DEC-22
25961|Jarlemai Siltstone|30897|6|Mentioned|p19|||Subsurface unit||||||
25961|Jarlemai Siltstone|31396|6|Mentioned|p1183|||||||||
25961|Jarlemai Siltstone|32648|6|Mentioned|p32|||U. Jur||||||
25961|Jarlemai Siltstone|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
25961|Jarlemai Siltstone|33166|6|Mentioned|p67|||Stratigraphy||||||
25961|Jarlemai Siltstone|33518|4|Described|Table 1|||||||||
25961|Jarlemai Siltstone|33519|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
25961|Jarlemai Siltstone|34134|6|Mentioned|Cor.Chart|||Upper Jurassic||||||
25961|Jarlemai Siltstone|34287|6|Mentioned|p178|||Jurassic||||||
25961|Jarlemai Siltstone|34363|6|Mentioned|p56|||See also Fig.7. Upper Jurassic||||||
25961|Jarlemai Siltstone|35152|6|Mentioned|p20|||||||||
25961|Jarlemai Siltstone|35275|6|Mentioned|Fig.5.|||||||||
25961|Jarlemai Siltstone|35711|4|Described|p26|||See also Table 3,stratigraphy||||||
25961|Jarlemai Siltstone|35969|6|Mentioned|p66|||||||||
25961|Jarlemai Siltstone|35983|6|Mentioned|Table 28|||||||||
25961|Jarlemai Siltstone|36224|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Mudstone, massive, bioturbated, sandy, glauconitic, phosphatic; minor limestone; fossiliferous.||||||01-FEB-05
25961|Jarlemai Siltstone|36257|6|Mentioned|Table 2.1|||||||||
25961|Jarlemai Siltstone|36634|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
25961|Jarlemai Siltstone|36890|3|Fully described|p347|||||||||
25961|Jarlemai Siltstone|37364|6|Mentioned|p1051|||||||||
25961|Jarlemai Siltstone|37368|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
25961|Jarlemai Siltstone|37369|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
25961|Jarlemai Siltstone|37370|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
25961|Jarlemai Siltstone|37564|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
25961|Jarlemai Siltstone|38149|6|Mentioned|p87|||||||||
25961|Jarlemai Siltstone|38444|6|Mentioned|p301|||||||||
25961|Jarlemai Siltstone|38878|6|Mentioned|Map legend|Tithonian|Kimmeridgian|Oxfordian - Neocomian||||||
25961|Jarlemai Siltstone|38886|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Early Cretaceous to Late Jurassic||||||
25961|Jarlemai Siltstone|39857|6|Mentioned|Map legend|Late Cretaceous|Late Jurassic|Early Cretaceous to Late Jurassic||||||
25961|Jarlemai Siltstone|40045|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
25961|Jarlemai Siltstone|40078|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
25961|Jarlemai Siltstone|40992|6|Mentioned|Fig.11|||||||||
25961|Jarlemai Siltstone|41169|6|Mentioned|Fig.3|||||||||
25961|Jarlemai Siltstone|41436|6|Mentioned|p46|||||||||
25961|Jarlemai Siltstone|41639|6|Mentioned|p14|||||||||
25961|Jarlemai Siltstone|41730|6|Mentioned|Fig.3|||||||||
25961|Jarlemai Siltstone|42338|5|Briefly described|Table 1 P145|||||||||
25961|Jarlemai Siltstone|42571|5|Briefly described|p17|||||||||
25961|Jarlemai Siltstone|42572|5|Briefly described|Map Legend|Jurassic||||||||23-DEC-09
25961|Jarlemai Siltstone|42792|5|Briefly described|Table 1 P225|||||||||
25961|Jarlemai Siltstone|42814|5|Briefly described|p24|||||||||
25961|Jarlemai Siltstone|42930|5|Briefly described|Fig.1 p473|Early Carboniferous|Early Carboniferous|Conformably overlies Alexander Formation; unconformably underlies Broome Sandstone. Geological Province: Canning Basin. Shallow, marine deposits.||||||13-NOV-07
25961|Jarlemai Siltstone|43173|5|Briefly described|13|Early Cretaceous|Late Jurassic|||||||
25961|Jarlemai Siltstone|43563|6|Mentioned|Fig.2,p5||Late Jurassic|||||||
25961|Jarlemai Siltstone|43666|6|Mentioned|p45,Table 2||Tithonian|||||||
25961|Jarlemai Siltstone|43746|6|Mentioned|Fig.2,p11|Tithonian|Kimmeridgian|||||||
25961|Jarlemai Siltstone|43818|6|Mentioned|Fig.2.p39||Late Jurassic|||||||
25961|Jarlemai Siltstone|44040|14|Not recorded|p43|||||||||
25961|Jarlemai Siltstone|44143|4|Described|p.433 Table 4-19; p.449|Jurassic|Jurassic|259m thick in Barlee 1; mudstone, massive, sandy in parts; shallow marine. Conformably overlies Alexander Formation; conformably(?) overlain by Broome and Mowla Sandstones; unconformably or disconformably overlain by Callawa Formation. Type section at Mount Jarlemai (MOUNT ANDERSON: 18deg 42' 55" S, 123deg 48' 40" E). Microfossils, bivalves, belemnites, ammonites and brachiopods. Also appears as Jarleman Siltstone on p449.||||||23-NOV-17
25961|Jarlemai Siltstone|44357|4|Described|p13,Tb.1 p9||Jurassic|Subsurface only.||||||
25961|Jarlemai Siltstone|44443|5|Briefly described|map legend|Early Cretaceous|Late Jurassic|||||||
25961|Jarlemai Siltstone|44997|14|Not recorded|p.36,38,41,43,52|||||||||
25961|Jarlemai Siltstone|44998|2|Defined|p147||Jurassic|Conformably overlies Alexander Formation. Overlain by Mowla Sandstone. Correlates with "Broome Buchia Beds". On many pages. p.119,131-3,146-9,154,182,188, map.||||||
25961|Jarlemai Siltstone|45153|2|Defined|App.6-101|Late Jurassic|Late Jurassic|Also known as Jarlemai Formation.||||||26-JUL-07
25961|Jarlemai Siltstone|45158|3|Fully described|p14|||||||||
25961|Jarlemai Siltstone|46319|4|Described|p18|Late Jurassic|Late Jurassic|Geological Province: Canning Basin.||||||
25961|Jarlemai Siltstone|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
25961|Jarlemai Siltstone|48596|14|Not recorded|p.5|||(E51-11)||||||
25961|Jarlemai Siltstone|48848|14|Not recorded|p.80,91|||||||||
25961|Jarlemai Siltstone|50189|6|Mentioned|p28|||On the COORAGOORA sgeet. May be acorrelative of the Callawa Formation.||||||
25961|Jarlemai Siltstone|50544|5|Briefly described|p62|Jurassic|Jurassic|Shallow marine deposits.  Not on the YARRIE sheet.  Geological Province: Northern Carnarvon Basin.||||||11-OCT-04
25961|Jarlemai Siltstone|50555|5|Briefly described|Map legend|Cretaceous|Jurassic|Mudstone and minor sandstone lenses. Geological Province: Canning and Northern Carnarvon Basins (Westralian Superbasin).||||||01-JUL-08
25961|Jarlemai Siltstone|60997|5|Briefly described|p138|Jurassic|Jurassic|Geological Province: Canning Basin (WA)||||||
25961|Jarlemai Siltstone|61021|5|Briefly described|p36 Fig. 2|Tithonian|Kimmeridgian|Geological Province: Canning Basin.||||||17-DEC-07
25961|Jarlemai Siltstone|63420|5|Briefly described|Map legend|Cretaceous|Jurassic|Mudstone and siltstone; minor sandstone (sub-surface only).||||||
25961|Jarlemai Siltstone|64186|5|Briefly described|p171, p170 Fig. 1|Tithonian|Tithonian|Underlain by Alexander Formation, overlain by Broome Sandstone. Max thickness: 90m.||||||
25961|Jarlemai Siltstone|64580|4|Described|map legend||Late Jurassic|Mudstone, siltstone; minor sandstone locally.||||||09-DEC-08
25961|Jarlemai Siltstone|64643|5|Briefly described|p3 Fig. 2|Late Jurassic|Late Jurassic|||||||10-FEB-20
25961|Jarlemai Siltstone|64982|6|Mentioned|p700.|||||||||
25961|Jarlemai Siltstone|65301|5|Briefly described|p5 Fig. 4|Late Jurassic|Late Jurassic|Geological province: Canning Basin.||||||
25961|Jarlemai Siltstone|65449|6|Mentioned|p6|Late Jurassic|Late Jurassic|||||Overlies Alexander Formation. Is overlain unconformably by Broome Sandstone and Callawa and Cronin Formations.||
25961|Jarlemai Siltstone|66949|6|Mentioned|p34|Early Cretaceous|Late Jurassic||||||Includes extremely thin coal seams.|
25961|Jarlemai Siltstone|67202|6|Mentioned|p44 Fig.2.10|||Canning Basin. An aquiclude.||||Unconformably overlain by the Wallal Sandstone. Overlain by the Broome Sandstone.||15-FEB-18
25961|Jarlemai Siltstone|68007|6|Mentioned|p4, p7-8|Late Jurassic|Late Jurassic|Canning Basin. Interpreted as 22m thick in Patience 1 well (200-222m depth), Menzel and Lipski (1986). No biostratigraphic data presented.||||||19-FEB-20
25961|Jarlemai Siltstone|68283|5|Briefly described|Map Legend|Cretaceous|Jurassic|Canning Basin.|||||Mudstone and siltstone; minor sandstone (subsurface only).|
25961|Jarlemai Siltstone|68811|5|Briefly described|p78, p79, p173 tbl 34|Cretaceous|Jurassic|Acts as an aquiclude beneath the Broome Sandstone. ||||Unconformably overlain by the Broome Sandstone.|Siltstone and claystone with minor sandstone and sandy siltstone.|14-APR-20
25961|Jarlemai Siltstone|68902|6|Mentioned|p9 fig 5|Jurassic|Jurassic|||||Overlies Alexander Formation. Is overlain unconformably by Broome Sandstone.||19-FEB-20
25961|Jarlemai Siltstone|69029|6|Mentioned|p319|Tithonian|Kimmeridgian|Of Canning Basin.||||Overlain by Bardwire Sandstone. Underlain by Alexander Formation.||
25961|Jarlemai Siltstone|69182|6|Mentioned|Ch4 p3, Ch4 p9, Ch4 p30-p35|Upper Jurassic|Upper Jurassic|Incorrectly labelled as the (now obsolete) Jarlemai Formation in Ch4 p9. See also Ch4 p45, Ch4 p64, Ch4 p83-p84.  ||||Overlies the Alexander Formation. Unconformably overlain by the Broome Sandstone.||
25961|Jarlemai Siltstone|69297|6|Mentioned|p337, p352|Berriasian|Tithonian|Broome Platform of the Canning Basin. ||||Overlies the Alexander Formation. Unconformably overlain by the Mowla Sandstone.||
25961|Jarlemai Siltstone|69312|5|Briefly described|p3|Tithonian|Kimmeridgian|Canning Basin. ||||Overlies the Alexander Formation. Unconformably (or disconformably) overlain by the Broome or Barbwire Sandstones.|Shale with minor carbonate interbeds.|
25961|Jarlemai Siltstone|70154|5|Briefly described|500k_interpgeop14_lut.csv|Upper Jurassic|Kimmeridgian||145-157 Ma||||Mudstone, siltstone; minor sandstone locally.|13-DEC-22
25961|Jarlemai Siltstone|70774|5|Briefly described|p4|Late Jurassic|Late Jurassic|Canning Basin.||||Overlies the Alexander Formation. Unconformably overlain by the Broome Sandstone, Callawa and Cronin Formations.||10-FEB-20
25961|Jarlemai Siltstone|70826|6|Mentioned|p7 tbl 4|Early Cretaceous|Jurassic|Canning Basin.||||||
25961|Jarlemai Siltstone|71267|4|Described|GEOL_LUT_CSV files|Late Jurassic|Kimmeridgian|Of Canning Basin. See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|157.3-145 Ma (biostrat)||||Shallow marine laminated pink and purple siltstone with a sugary texture, massive and partly sandy mudstone, limestone|
25961|Jarlemai Siltstone|72034|5|Briefly described|500k_interpgeop16_lut|Late Jurassic|Kimmeridgian|Canning Basin.  Age from biostratigraphy.|||||Mudstone, siltstone; minor sandstone locally.|
25961|Jarlemai Siltstone|72497|5|Briefly described|p3 Fig.2.|Tithonian|Kimeridgian|Shown as occuring in the Anketell, Tabletop, Ryan Shelves, Willara and Kidson Sub-basins, the Jurgurra and Barbwire Terraces and Broome Platform. Also shown as occuring in the Fitzroy Trough, Betty and Balgo Terraces and part of the Lennard Shelf and Margaret Terrace.||||Conformably overlies Alexander formation and laterally equivalent in part to Barbwire and Meda Sandstone.||
25961|Jarlemai Siltstone|73117|5|Briefly described|p3|Upper Jurassic|Upper Jurassic|Canning Basin. Upper boundary marked by the Breakup Unconformity that represents Jurassic-Cretaceous extensional events offshore.||||Underlain by Alexander Formation. Unconformably overlain by Callawa/Cronin formations and Broome Sandstone.|Dominantly shale and mudstone with lesser sandstone.|
80043|Jasper Hill Leucogranite|67198|6|Mentioned|p71|||Cuts across S1 planar fabric in the supracrustal cover of the Raeside dome. Leonora district, Eastern Goldfield Superterrane.|c.2741 Ma|||||22-SEP-17
80043|Jasper Hill Leucogranite|73596|6|Mentioned|p1164|Neoarchean|Neoarchean|Kalgoorlie-Kurnalpi Rift. Appears informally as Jasper Hill leucogranite.|2741 +/- 5 Ma (Baggott, 2006).|||||
75575|Jawilga beds|65074|4|Described|p351 fig 4-37, p351, p353, p357 Tb. 4-12|Neoproterozoic|Neoproterozoic|Of NW Birrindudu Basin. The reference area is 8km WNW of Pyramid Hill. Over 130m thick.||||Equivalent to Murraba Formation. Probably conformably overlies Denison beds and is overlain unconformably by Boee beds.|Conglomerate, sublithic arenite.|
75575|Jawilga beds|69440|5|Briefly described|p25:1-3|Cryogenian|Cryogenian|Crops out on both sides of a major anticline between Baines Hill and Denison Range in BILLILUNA map area. The conglomerate is similar to the Murraba Formation.||||Conformably overlies Denison beds. Is overlain conformably by Boee beds. Correlates with Murraba Formation (NT).|Conglomerate, fine- to medium-grained sublithic arenite and thinly bedded, chert granule conglomerate.|12-JUL-16
75575|Jawilga beds|71080|6|Mentioned|p4|||Of Blake et al. 1977, 1979. Previously considered potential correlative of Murraba Formation. ||||||
75575|Jawilga beds|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Partly cross bedded medium to fine grained lithic sandstone and chert granule conglomerate|
68517|Jean Well Granodiorite|63441|2|Defined|p10 Tb. 2|Archean|Archean|Of the Maitland River Supersuite. Unconformable below Hardey Formation. Intrudes Cliff Pool Tonalite; intruded by Munni Munni Intrusion. Ages: 2985+/-7Ma, 2988+/-4Ma and 2990+/-3Ma. Geological province: Pilbara Craton.||||||07-FEB-11
68517|Jean Well Granodiorite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Maitland River Supersuite. Geological province: Pilbara Craton.  Granodiorite and lesser monzogranite; foliated and weakly compositionally banded; locally sparsely porphyritic; metamorphosed.||||||07-NOV-08
68517|Jean Well Granodiorite|64580|4|Described|map legend||Mesoarchean|Of Maitland River Supersuite. Foliated, weakly compositionally banded, and locally sparsely porphyritic granodiorite and lesser monzogranite; metamorphosed.||||||15-DEC-08
68517|Jean Well Granodiorite|67201|4|Described|p16-17 Fig.9|Archean|Archean|Pilbara Draton. In Roebourne-Karratha area.||Maitland River Supersuite|||Granodiorite and lesser monzogranite; foliated and weakly compositionally banded; locally sparsely porphyritic; metamorphosed.|
68517|Jean Well Granodiorite|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Maitland River Supersuite.|||Foliated, weakly compositionally banded, and locally sparsely porphyritic granodiorite and lesser monzogranite; metamorphosed|
68517|Jean Well Granodiorite|70775|5|Briefly described|p15, p53|Mesoarchean|Mesoarchean|Pilbara Craton. Together with the Toorare Tonalite, Whyjabby Granodiorite, Brill Monzogranite, Waloo Waloo Monzogranite and Mardeburra Granodiorite comprises the Cherratta Granitic Complex. This unit outcrops south and north of the Munni Munni Intrusion and in the area east of Karratha Homestead.|c. 2990 to 2988 Ma (SHRIMP, Nelson 1999c/d)|Maitland River Supersuite|||Granodiorite and lesser monzogranite; foliated and weakly compositionally banded; locally sparsely porphyritic; metamorphosed.|
68517|Jean Well Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, granodiorite|
68517|Jean Well Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|De Grey Superbasin.|Max age 2990+/-3 Ma, min 2985+/-7 Ma.|Maitland River Supersuite|||Granodiorite and lesser monzogranite; foliated and weakly compositionally banded; locally sparsely porphyritic; metamorphosed.|
27167|Jeeaila Sandstone Member|23723|4|Described|p9 Table 1|Mesoproterozoic|Mesoproterozoic|Of Bangemall Group. Overlying unit Fords Creek Shale. U'lying unit Coodardoo Formation. Geological Province: Bangemall Basin. Max. thickness: 80 m.||||||
27167|Jeeaila Sandstone Member|24183|6|Mentioned|p21|||Equivalent of the Backdoor Formation, middle (Chuck 1984)||||||
27167|Jeeaila Sandstone Member|35639|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27167|Jeeaila Sandstone Member|40089|2|Defined|p37|Mesoproterozoic|Mesoproterozoic|||||||
27167|Jeeaila Sandstone Member|41360|6|Mentioned|p192|||||||||
27167|Jeeaila Sandstone Member|44142|5|Briefly described|p312 Tb.4-4|||Shallow-marine turbidites, partly reworked by bottom currents. Up to 80m thick. Within Dooley Subgroup of Chuck (1984).||Fords Creek Shale.|||Medium-grained arenite (shallow marine turbidites, partly reworked by bottom currents).|13-MAR-18
27167|Jeeaila Sandstone Member|64728|6|Mentioned|pp106-107.|||||||A correlative of sampled part of  Backdoor Formation.||16-SEP-14
27167|Jeeaila Sandstone Member|66107|6|Mentioned|p5 |Mesoproterozoic|Mesoproterozoic|||||||
27167|Jeeaila Sandstone Member|67374|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Collier Basin.||Unit in Backdoor Formation.|||Thin- to very thick-bedded sandstone and minor siltstone.|
27167|Jeeaila Sandstone Member|68286|5|Briefly described|Map Legend|Stenian|Calymmian|Collier Basin.||Of the Backdoor Formation|||Thin to very thick bedded sandstone and minor siltstone.|
27167|Jeeaila Sandstone Member|69166|4|Described|geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|||Collier Group|||Thin to very thick bedded sandstone and minor siltstone|
40768|Jeedamya Complex|24196|5|Briefly described|p8|Archean|Archean|Age: 2681 +/- 4 Ma (Nelson, 1996). Geological Province: Yilgarn Craton.||||||07-NOV-08
40768|Jeedamya Complex|24494|5|Briefly described|p14|Archean|Archean|Age: 2681 +/- 4 Ma (U-Pb; Nelson, 1996). Calc-alkaline intermediate-silicic complex consisting of predominantly rhyolitic to rhyodacitic pyroclastic and volcaniclastic clasts.||||||07-NOV-08
40768|Jeedamya Complex|63980|4|Described|p73, 63.|Archean|Archean|Gindalbie Terrane. See also Jeedmya Rhyolite p64. Calc-alkaline intermediate-silicic volcanism. These rhyolites define a range from HFSE-enriched to compositions more typical of arc-related suites.|2681 +/- 5 Ma (Nelson 1997b).||||Basalt to andesite, defining a tholeiitic Fe-enrichment trend with respect to AFM components; rhyolites, less evolved and with lower concentrations of incompatible elements.|26-SEP-14
40768|Jeedamya Complex|65264|5|Briefly described|p9-10|||Geological province: Ginbaldie terrane. Calc-alkaline intermediate silicic complex consisting predominantly of rhyolitic to rhyodacitic pyroclastic and volcaniclastic rocks.||||||07-FEB-11
40768|Jeedamya Complex|69152|5|Briefly described|geochron file 110225.1.pdf|Neoarchean|Neoarchean|Dacite from this unit was dated with crystallisation age: 2681+/-4 Ma. In geochron file 110225.1.pdf from ?1997.||||||
40768|Jeedamya Complex|70153|5|Briefly described|110225.1.pdf|Archean|Archean|Age derived from meta-dacitic ignimbrite sample (110225.1.pdf)|2681 Ma +/- 4 Ma (SHRIMP)||||Includes a meta-ignimbrite porphyry.|
40768|Jeedamya Complex|73391|6|Mentioned|p286|||Gindalbie Terrane. Geochemical similarities with rhyolites in the Kalgoorlie Terrane, and lithological similarities, cast doubt on the Mount Monger Fault as a terrane boundary.||||||
72704|Jenkin Granodiorite|64621|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite. Biotite granodiorite, medium- to coarse-grained, foliated; metamorphosed.||||||07-NOV-08
72704|Jenkin Granodiorite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Emu Pool Supersuite. 3313-3307 Ma. Biotite granodiorite; medium- to coarse-grained; foliated; metamorphosed.||||||
72704|Jenkin Granodiorite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Emu Pool Supersuite|||Biotite granodiorite; medium- to coarse-grained; foliated; metamorphosed.|
72704|Jenkin Granodiorite|69566|6|Mentioned|p236|||Mount Edgar Granitoid Complex, East Pilbara Granite-Greenstone Terrane.||Emu Pool Supersuite.||||
72704|Jenkin Granodiorite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3310-3307 Ma (isotopic)|Unit of Emu Pool Supersuite.|||Biotite granodiorite; medium- to coarse-grained; foliated; metamorphosed|
72704|Jenkin Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite|
72704|Jenkin Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||Max age 3313+/-2 Ma, min 3307+/-3 Ma.|Emu Pool Supersuite|||Biotite granodiorite; medium to coarse grained; foliated; metamorphosed.|
31476|Jervoise Sandstone|12758|4|Described|p19, p10 Fig. 10|Early Cretaceous|Early Cretaceous|Previously informally referred to as the "Lower Parmelia Sandstone". Of the Parmelia Group. Conformably overlain by Stragglers Member; conformably overlies the Otowiri Formation.  Thickness in type section: 863m. Geological Province: Vlaming Sub-basin.||||||01-OCT-08
31476|Jervoise Sandstone|24443|5|Briefly described|Fig.31|Early Cretaceous|Late Jurassic|Of Parmelia Group. Conformably overlies Otorowiri Formation. Conformably overlain by Carnac Formation. Geological Province: Perth Basin.||||||
31476|Jervoise Sandstone|50108|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Parmelia Group.  Geological Province: Perth Basin.||||||
31476|Jervoise Sandstone|60376|5|Briefly described|p17 Fig. 4.|Late Jurassic|Late Jurassic|Geological Province: Perth Basin. Of the Parmelia Group. Overlian by Carnac Formation. Underlain by Otorowiri Formation.||||||07-FEB-11
31476|Jervoise Sandstone|69081|6|Mentioned|p736 Tb.1|||Geol. Prov: Perth Basin||||||
31476|Jervoise Sandstone|69182|6|Mentioned|Ch2 p15|Lower Cretaceous|Lower Cretaceous|Perth Basin. ||Parmelia Group||||
31476|Jervoise Sandstone|69297|6|Mentioned|p175, p189|Berriasian|Tithonian|Vlaming Sub-basin, South Perth Basin. ||Parmelia Group||||
31476|Jervoise Sandstone|70097|5|Briefly described|p19 Fig.3|Berriasian|Berriasian|Southern Perth Basin. Vlaming Sub-basin and Bunbury Trough.||Parmelia Group||Overlies Otorowiri Formation. Is overlain by Carnac Formation.|Sandstone.|12-SEP-17
31476|Jervoise Sandstone|70099|6|Mentioned|Fig.4|Berriasian|Berriasian|||Parmelia Group.||||
31476|Jervoise Sandstone|70128|5|Briefly described|p463 Fig.10|Early Cretaceous|Early Cretaceous|Vlaming Sub-basin.||Parmelia Group.||Overlies Otorowiri Formation. Is overlain by Carnac Formation.||
31476|Jervoise Sandstone|71377|5|Briefly described|p7|Early Cretaceous|Late Jurassic|Bunbury Trough, Perth Basin.||Parmelia Group||||
31476|Jervoise Sandstone|71958|5|Briefly described|p15, p34, p41, p45-p46, p51, p58, p80|Kimmeridgian|Oxfordian|Vlaming Sub-basin.||Parmelia Group||Unconformably overlain by the Warnbro Group. Overlies the Otorowiri Foramtion. Overlain by the Carnac Formation.|Sandstones.|
24641|Jinduckin Formation|9324|5|Briefly described|Map Legend|Ordovician|Cambrian|Of the Daly River Group. Quartz arenite, coarse friable, ripple-marked; minor limestone lenses.||||||
24641|Jinduckin Formation|22809|5|Briefly described|21|||||||||
24641|Jinduckin Formation|22810|4|Described|Table3 P7, P19|Ordovician|Cambrian|Overlies Tindall Limestone||||||
24641|Jinduckin Formation|22813|5|Briefly described|Map|Ordovician|Cambrian|Maroon dolomitic-siliclastic siltstone and dolomitic sandstone-siltstone interbeds.||||||19-OCT-05
24641|Jinduckin Formation|23216|4|Described|p4,Table1p7,38,42-5|Tremadoc|Late Cambrian|Of the Daly River Group.||||||19-JAN-06
24641|Jinduckin Formation|23373|6|Mentioned|p318|||of Daly Basin.||||||
24641|Jinduckin Formation|23714|5|Briefly described|p7 Table 1.|Paleozoic|Paleozoic|See also page 36. Of Daly River Group. Max. thickness: 350 m.||||||07-NOV-08
24641|Jinduckin Formation|23715|5|Briefly described|Map legend||Paleozoic|||||||07-NOV-08
24641|Jinduckin Formation|24122|3|Fully described|p13, p3 Fig. 2|Early Ordovician|Middle Cambrian|Of Daly River Group. Conformably overlies Tindall Limestone. Maximum thickness: 356m (on PINE CREEK). Sandstone, siltstone, marl, carbonates.  Geological Province: Daly Basin.||||||
24641|Jinduckin Formation|24300|5|Briefly described|Map Legend|Ordovician|Cambrian|Parent: Daly River Group.   Geological Province: Daly Basin||||||
24641|Jinduckin Formation|24303|4|Described|p39, p41|Early Ordovician|Late Cambrian|Geological Province: Daly Basin. Lithological similarities with Middle Cambrian units, Wonarah beds and Burton beds (Georgina Basin) suggest possibility of Middle Cambrian age for this unit?||||||
24641|Jinduckin Formation|24334|5|Briefly described|p48 Tb.1|Arenig|Late Cambrian|Age: 470 - 495 Ma||||||
24641|Jinduckin Formation|29591|6|Mentioned|p107|||||||||
24641|Jinduckin Formation|30659|6|Mentioned|p91|||||||||
24641|Jinduckin Formation|30660|6|Mentioned|Table 1|||Lower Ordovician age||||||
24641|Jinduckin Formation|30661|6|Mentioned|Table 1|||||||||
24641|Jinduckin Formation|30662|6|Mentioned|p188|||Palaeomagnetic dates||||||
24641|Jinduckin Formation|31572|6|Mentioned|p22|||L.Ordovician. Correlation chart||||||
24641|Jinduckin Formation|31917|5|Briefly described|p33|||Early Ordovician. See Fig.2,4||||||
24641|Jinduckin Formation|32107|6|Mentioned|p409|||Palaeomagnetic results||||||
24641|Jinduckin Formation|32170|6|Mentioned|Map legend|Early Ordovician|Middle Cambrian|Middle Cambrian - Lower Ordovician||||||
24641|Jinduckin Formation|32171|6|Mentioned|p8|||Middle Cambrian||||||
24641|Jinduckin Formation|32700|4|Described|Table 2|||See also P16. Refers Randal (1962)||||||
24641|Jinduckin Formation|32775|5|Briefly described|Map legend|Early Ordovician|Middle Cambrian|Sandstone, siltstone, marl, carbonate beds.||||||02-DEC-04
24641|Jinduckin Formation|33373|3|Fully described|p12|||Table 3.||||||
24641|Jinduckin Formation|33376|6|Mentioned|Map legend|Early Ordovician|Middle Cambrian|Middle Cambrian to Lower Ordovician||||||
24641|Jinduckin Formation|33738|6|Mentioned|p48|||||||||
24641|Jinduckin Formation|34438|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian or Ord.||||||
24641|Jinduckin Formation|34439|4|Described|Table 1|||Camb. or Ord. See also PP9,11,13,14||||||
24641|Jinduckin Formation|35088|6|Mentioned|Fig.8|||||||||
24641|Jinduckin Formation|36138|6|Mentioned|Table 1|||||||||
24641|Jinduckin Formation|36335|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
24641|Jinduckin Formation|37818|6|Mentioned|Table 2|||||||||
24641|Jinduckin Formation|39210|5|Briefly described|Fig.18|||||||||
24641|Jinduckin Formation|40128|6|Mentioned|p1|||||||||
24641|Jinduckin Formation|40136|5|Briefly described|p28|||||||||
24641|Jinduckin Formation|40168|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician. Of the Daly River Group. Limestone (stromatolitic in places), calcareous sandstone, sandy limestone, quartz sandstone, siltstone, shale.||||||18-OCT-05
24641|Jinduckin Formation|40957|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
24641|Jinduckin Formation|42012|2|Defined|p43|Early Ordovician|Middle Cambrian|See also p21.||||||28-SEP-06
24641|Jinduckin Formation|42014|5|Briefly described|Map legend|Ordovician||||||||
24641|Jinduckin Formation|42070|4|Described|p3|||||||||
24641|Jinduckin Formation|43011|6|Mentioned|Table 2,p12|||||||||
24641|Jinduckin Formation|43140|5|Briefly described|p4|||of Daly River Group.||||||
24641|Jinduckin Formation|43149|5|Briefly described|Map Legend||Cambrian|of Daly River Group||||||
24641|Jinduckin Formation|43832|4|Described|31, Table7 p26|Early Ordovician|Late Cambrian|Contains late Tremadocian - basal Arenig conodont zones||||||
24641|Jinduckin Formation|44113|5|Briefly described|p240|Early Ordovician|Middle Cambrian|Of the Daly River Group. Geological Province: Daly River Basin. Maximum Thickness: 397m.||||||
24641|Jinduckin Formation|44201|14|Not recorded|p.10|||||||||
24641|Jinduckin Formation|45058|5|Briefly described|p19|||Unit of Daly River Gp.||||||
24641|Jinduckin Formation|45064|3|Fully described|Table 1|||See also p21.||||||28-SEP-06
24641|Jinduckin Formation|45148|6|Mentioned|Fig.4|||Daly River Basin||||||
24641|Jinduckin Formation|46675|5|Briefly described|Map legend|Paleozoic|Paleozoic|Of the Daly River Group.  Siltstone and silty shale with minor sandstone and chert.||||||07-NOV-08
24641|Jinduckin Formation|46676|14|Not recorded|p.6||Middle Cambrian|M.Cambrian; unit of Daly River Group.||||||
24641|Jinduckin Formation|46679|14|Not recorded|map legend||Middle Cambrian|Middle Cambrian.||||||
24641|Jinduckin Formation|48942|3|Fully described|p82|||Strat. section p117.||||||28-SEP-06
24641|Jinduckin Formation|64068|5|Briefly described|p8|||Daly Basin. Paleopoles from this (and other) units define a major change in APWP.||||||
24641|Jinduckin Formation|64975|6|Mentioned|p162 Fig.6.|Cambrian|Cambrian|||||||
24641|Jinduckin Formation|65339|5|Briefly described|p5 Fig.4. |||||Unit in Daly River Group.|||Sandstone, shale, dolostone.|
24641|Jinduckin Formation|65342|5|Briefly described|p8.|||Beetaloo Sub-basin, Dunmarra Basin. Max. thickness at least 205 m.||||Overlies Tindall Limestone.|Sandstone-siltstone interbeds, dolostone; evaporite common in siltstone and some sandstone.|
24641|Jinduckin Formation|65345|5|Briefly described|p4.|||||Unit in Daly River Group.|||Dolomitic siltstone, dolostone and dolomitic quartz sandstone.|
24641|Jinduckin Formation|67186|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Daly River Group||Overlies Tindall Limestone.|Quartz sandstone, coarse, friable, ripple-marked; minor limestone lenses.|23-NOV-11
24641|Jinduckin Formation|69018|6|Mentioned|p450 Fig.1b|||||||||
24641|Jinduckin Formation|69437|5|Briefly described|p22:10-11|Series 3|Series 3|Daly Basin, Centralian B Superbasin. Sequence 2. Lithologically very similar to Anthony Lagoon Formation (Barkly Sub-basin).||||Overlies Tindall Limestone. Is overlain by Oolloo Dolostone.||12-JUL-16
24641|Jinduckin Formation|69443|5|Briefly described|p28:22|Middle Cambrian|Middle Cambrian|Daly Basin. Correlation, based on striking similarity, has this unit regarded as Middle Cambrian.||||Correlated with Anthony Lagoon Formation. Is overlain by Oolloo Dolostone.||12-JUL-16
24641|Jinduckin Formation|69446|4|Described|p31:1-7, 9, 11|Middle Cambrian|Middle Cambrian|Daly Basin. Up to 356.1m thick; is 335.4m thick in the type section in drillhole NTGS 86/1. Low- to moderate-energy peritidal, tidal flat deposits. Features include nodular anhydrite, halite hopper casts and secondary gypsum veins, mudcracks and/or burrows, flat-pebble breccias, intraformational conglomerate, soft-sediment deformation, stromatolites. Unsuccessfully explored for uranium.||Daly River Group.||Conformably, locally disconformably overlies Tindall Limestone. Is overlain conformably/transitionally by Oolloo Dolostone. Lithologically correlated with Anthony Lagoon Formation (Georgina Basin).|Maroon-green dolomitic-siliciclastic siltstone, dolomitic sandstone-siltstone interbeds, ooid dolograinstone, microbial dolostone; dolomitic quartz sandstone in upper part.|12-JUL-16
24641|Jinduckin Formation|69447|6|Mentioned|p32:2|||Daly Basin.||||Broadly correlated with Point Wakefield beds (Wiso Basin).||12-JUL-16
24641|Jinduckin Formation|69561|6|Mentioned|p33 fig 2, p33|Floran|Templetonian|In comparison to underlying Tindall Limestone is essentially unfossiliferous.||||Overlain by Oolloo Dolostone, overlies Tindall Limestone||
24641|Jinduckin Formation|69673|4|Described|p191|||356m thick.||Daly River Group||Overlain by Oolloo Dolostone, overlies Tindall Limestone|Siliciclastic siltstone with dolomitic sandstone-siltstone interbeds and local lenses of ooid dolograinstone, microbial dolostone and dolomitic quartz sandstone.|
24641|Jinduckin Formation|70380|3|Fully described|p743-746, p748-750, p752,p755,p757,p759|Drumian|Stage 5|Daly Basin. Unfossiliferous. Mistakenly thought to include Tremadocian to Floian conodonts, trilobites and brachiopods (Opik, 1968; Jones, 1971) and was mapped accordingly (Kruse et al., 1990, 1994). The strata containing those fossils was later recognised as a younger, separate unit, the Florina Formation. Up to 356.1m thick; is 335.4m thick in the type section in drillhole NTGS86/1. Correlated with Point Wakefield beds (Wiso Basin); also with Anthony Lagoon, Wonarah and Arthur Creek Formations (Georgina Basin). The lower contact represents a (carbonate-to-siliciclastic) major sequence boundary. Several sedimentary structures (listed). Peritidal sediments deposited on a prograding mixed carbonate-siliciclastic tidal flat.||Daly River Group.||Overlies Tindall Limestone conformably (possibly locally disconformably)[4 consecutive adverbs!!]. Is overlain transitionally by Oolloo Dolostone.|Mainly maroon-green dolomitic-siliciclastic siltstone with dolomitic sandstone-siltstone interbeds, and local lenses of ooid dolograinstone, microbial dolostone and, in its upper half, dolomitic quartz sandstone.|
24641|Jinduckin Formation|70850|5|Briefly described|Map legend.|Cambrian|Cambrian|Daly Basin.||Daly River Group.|||Sandstone, siltstone, marl, carbonate.|
24641|Jinduckin Formation|70866|5|Briefly described|Map legend.|Cambrian|Cambrian|Daly Basin.||Daly River Group.||Conformably overlies Tindall Limestone. Is overlain conformably by Oolloo Dolostone.|Dolomitic-siliciclastic siltstone with sandstone-siltstone interbeds; quartz sandstone; dolostone; minor cryptalgal dolostone, ooid dolograinstone and dolomitic quartz sandstone; evaporite (mainly anhydrite), common locally; flat-pebble breccia.|
24641|Jinduckin Formation|70968|6|Mentioned|p75|Cambrian|Cambrian|Fence diagram of wells in Beetaloo Sub-basin.||||||
24641|Jinduckin Formation|73083|6|Mentioned|p39|||||||||
25964|Jingemia Dolomite|23761|5|Briefly described|p11|||Parent: Moora Group||||||
25964|Jingemia Dolomite|23762|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Moora Group.||||||
25964|Jingemia Dolomite|24160|6|Mentioned|p26, p27 Tb.14|Proterozoic|Proterozoic|||Coomberdale Subgroup||||
25964|Jingemia Dolomite|24410|5|Briefly described|p139|Proterozoic|Proterozoic|Of the Coomberdale Subgroup (Moora Group). ?Superseded Coomberdale Chert and Dudawa Beds. See also p142 Tb. 60.||||||24-NOV-09
25964|Jingemia Dolomite|40307|6|Mentioned|p64|||||||||
25964|Jingemia Dolomite|40346|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25964|Jingemia Dolomite|40347|2|Defined|p22|Proterozoic|Proterozoic|||||||
27168|Joffre Member|23045|5|Briefly described|289|||Of Brockman Iron Formation.||||||
27168|Joffre Member|23046|6|Mentioned|184|||||||||
27168|Joffre Member|23126|5|Briefly described|p383 Fig.3|||||||||
27168|Joffre Member|23194|6|Mentioned|p41|||Hamersley Group.||||||
27168|Joffre Member|23536|5|Briefly described|p 427|||||||||
27168|Joffre Member|23612|5|Briefly described|p845 Fig 5|||Of Brockman Iron Formation||||||
27168|Joffre Member|24041|4|Described|p492|Paleoproterozoic|Paleoproterozoic|Of the Brockman Iron Formation.||||||07-NOV-08
27168|Joffre Member|24047|6|Mentioned|p19|||Of the Brockman Formation.||||||
27168|Joffre Member|24231|5|Briefly described|p186 Fig.2|||Geological Province: Hamersley Basin.||||||
27168|Joffre Member|24426|5|Briefly described|p218 Fig.3|Paleoproterozoic|Archean|Of Brockman Iron Formation. Overlies Whaleback Shale Member. Overlain by Yandicogina Shale Member. Geological Province: Hamersley Province.||||||07-FEB-11
27168|Joffre Member|24544|4|Described|p57 Fig.43|Paleoproterozoic|Paleoproterozoic|Of Brockman Iron Formation. Overlies Whaleback Shale Member. Overlain by Yandicoogina Shale Member. Banded iron-formation. Geological Province: Hamersley Basin.||||||27-MAY-16
27168|Joffre Member|29629|5|Briefly described|p899|||||||||
27168|Joffre Member|29716|4|Described|Table 1|||||||||
27168|Joffre Member|30437|6|Mentioned|p98|||||||||
27168|Joffre Member|30488|6|Mentioned|p89|||1720 +/- 25m.y. from beds of porcelanite. Refs Trendall & de Laeter(72).||||||
27168|Joffre Member|30685|5|Briefly described|p907|||Re mineralization||||||
27168|Joffre Member|31021|5|Briefly described|p893|||||||||
27168|Joffre Member|31670|4|Described|p913|||||||||
27168|Joffre Member|31671|5|Briefly described|p11|||||||||
27168|Joffre Member|32326|6|Mentioned|p122|||Important hematite ore bodies.||||||
27168|Joffre Member|33538|6|Mentioned|p291|||||||||
27168|Joffre Member|33540|6|Mentioned|p885|||||||||
27168|Joffre Member|33542|6|Mentioned|p412|||||||||
27168|Joffre Member|33544|2|Defined|p75|Precambrian|Precambrian|Previously Mindy Mindy Member.||||||07-APR-09
27168|Joffre Member|33545|5|Briefly described|p113|||||||||
27168|Joffre Member|33687|5|Briefly described|p918|||Also p921 re mineralzation||||||04-AUG-15
27168|Joffre Member|34541|4|Described|p53|||See also pp55-57||||||04-AUG-15
27168|Joffre Member|34542|4|Described|p94|||Originally Mindy Mindy Member.||||||
27168|Joffre Member|35052|6|Mentioned|Fig.2|||||||||
27168|Joffre Member|35260|5|Briefly described|Table 3|||||||||
27168|Joffre Member|35299|5|Briefly described|p893|||||||||
27168|Joffre Member|36091|5|Briefly described|p572|||||||||
27168|Joffre Member|36247|6|Mentioned|p187|||See also Fig.2.||||||
27168|Joffre Member|36260|5|Briefly described|p78|Paleoproterozoic|Paleoproterozoic|Of the Brockman Iron Formation. Geological Province: Hamersley Basin.||||||07-NOV-08
27168|Joffre Member|36642|6|Mentioned|Table 1|||||||||
27168|Joffre Member|36882|4|Described|p132|||||||||
27168|Joffre Member|37226|6|Mentioned|Fig.1|||||||||
27168|Joffre Member|37297|6|Mentioned|Fig.2|||||||||
27168|Joffre Member|37460|6|Mentioned|Fig.3.4|||||||||
27168|Joffre Member|37577|6|Mentioned|p30|||||||||
27168|Joffre Member|37704|6|Mentioned|Fig.1|||||||||
27168|Joffre Member|37708|6|Mentioned|p1930|||||||||
27168|Joffre Member|38790|6|Mentioned|p164|||||||||
27168|Joffre Member|39171|6|Mentioned|p80|||See also Fig.54||||||
27168|Joffre Member|39200|6|Mentioned|Fig.4|||||||||
27168|Joffre Member|39697|6|Mentioned|p126|||||||||
27168|Joffre Member|39952|5|Briefly described|p289|||||||||
27168|Joffre Member|41358|6|Mentioned|p148|||||||||
27168|Joffre Member|41768|5|Briefly described|p28|||||||||
27168|Joffre Member|42112|5|Briefly described|p9|||||||||
27168|Joffre Member|42190|6|Mentioned|p274|||||||||
27168|Joffre Member|42471|4|Described|p8|||of Brockman Iron Formation||||||
27168|Joffre Member|42495|6|Mentioned|p2|||||||||
27168|Joffre Member|42686|5|Briefly described|map legend|Proterozoic|Archean|||||||07-NOV-08
27168|Joffre Member|42743|5|Briefly described|map legend|Proterozoic|Archean|||||||07-NOV-08
27168|Joffre Member|42744|4|Described|p5|||of Brockman Iron Formation.||||||
27168|Joffre Member|43119|5|Briefly described|p10|||of Brockman Iron Formation||||||
27168|Joffre Member|43210|5|Briefly described|Table 1 p3,p5.||Mesoproterozoic|of Brockman Iron Formation.||||||
27168|Joffre Member|43262|5|Briefly described|Map Legend||Proterozoic|of Brockman Iron Formation.||||||
27168|Joffre Member|43290|5|Briefly described|p7||Proterozoic|of Brockman Iron Formation.||||||
27168|Joffre Member|44152|5|Briefly described|p179 Fig.2-155, p180, p182, p185-187|||Detailed comparison of this with similar BIF units of Hamersley Group on p185.||Brockman Iron Formation.||Overlies Whaleback Shale Member. Is overlain by Yandicoogina Shale Member.|BIF.|
27168|Joffre Member|50227|5|Briefly described|p442, p443 Fig. 1|Paleoproterozoic|Paleoproterozoic|BIF-rich unit of the Brockman Iron Formation (Hamersley Group).  Max. thickness: ~400m.  Age: 2459-2454Ma. Geological Province:  Hamersley Province.||||||07-FEB-11
27168|Joffre Member|60373|6|Mentioned|p145 Tb. 1|Archean|Archean|Of Brockman Iron Formation.||||||23-JUN-09
27168|Joffre Member|60706|4|Described|p623 Fig.2, p624,  p643 App.1|Paleoproterozoic|Paleoproterozoic|Of Brockman Iron Formation. Comprises of well-banded BIF made up of chert & iron oxides; 5 thin stipnomelane layers concordant with the stratification of the BIF.  Age: 2461+/-4 Ma, 2461+/-5 Ma, 2465+/-6 Ma (SHRIMP). Geological Province: Hamersley Basin.||||||07-NOV-08
27168|Joffre Member|62129|3|Fully described|p10|Archaean|Archaean|Of Brockman Iron Formation. Overlies Whaleback Shale Member. Thickness: 280m. Geological Province: Hamersley Basin. Consists of BIF with minor thin shale horizons.||||||07-FEB-11
27168|Joffre Member|63153|5|Briefly described|p1360, p1362 Fig.3. |||Simple broad-scale folding with visible cleavage or schistosity is characteristic.||Unit in Brockman Iron Formation.|||300 m thick BIF.|
27168|Joffre Member|64384|5|Briefly described|p35 Tb. 6, p36|||Of Brockman Iron Formation (Hamersley Group). Geological province: Hamersley Basin. Consists dominantly of BIF + thin shale layers.Ward et al (1975) identified an associated median shale-tuff zone informally called Ferro Gully shale.||||||07-FEB-11
27168|Joffre Member|64406|5|Briefly described|p1-2|||Of the Brockman Iron Formation. Overlies Whaleback Shale Member. Geological Province: Hamersley Basin.  Discussed in the context of its use as facing stone forming the lift panels in Mineral House, Perth.||||||29-SEP-08
27168|Joffre Member|64725|5|Briefly described|p58.||||c.2460 Ma (Pickard 2002).|Unit in Brockman Iron-formation.||Overlies Whaleback Shale Member.||
27168|Joffre Member|65683|5|Briefly described|p801 Fig2|||Of Brockman Iron Formation. Underlies Yandicoogina Shale Member; overlies Whaleback Shale Member.||||||08-MAR-12
27168|Joffre Member|65757|5|Briefly described|p84 Fig.2|||Banded iron formation, underlies the Yandicoogina Member, overlies the Mount Whaleback Member, part of the Brockman Iron Formation.||||||
27168|Joffre Member|67025|5|Briefly described|p319, p328.|||||Unit in Brockman Iron Formation.||Conformably overlies Whaleback Shale Member. Is overlain conformably by Yandicoogina Shale Member.||
27168|Joffre Member|67056|5|Briefly described|p419 Fig.2, p443. |||Does not show the marked BIF/non-BIF variation in lithologies that characterises the Dales Gorge Member and the Marra Mamba Iron Formation.||Unit in Brockman Iron Formation.||Overlies Mount Whaleback Shale. Is overlain by Yandicoogina Shale.||
27168|Joffre Member|67130|5|Briefly described|p3 fig 2, p8, p41|Siderian|Siderian||c. 2460 Ma|Brockman Iron Formation||Overlies Whaleback Shale Member, overlain by Yandicoogina Shale Member|Banded iron formation|
27168|Joffre Member|67201|4|Described|p34 Fig.18, p35, p52, p54, p56||||c 2454 Ma near top, U-Pb SHRIMP|Brockman Iron Formation||Overlies Whaleback Shale Member and is overlain by Weeli Wolli Formation.||
27168|Joffre Member|67721|5|Briefly described|p38 Fig.9|Siderian|Siderian|Approximately 360 m thick.|c. 2460 Ma|Of the Brockman iron formation.|||Banded iron formation; divided into six zones|
27168|Joffre Member|67827|6|Mentioned|p414 Fig.4, p415|||Wittenoom. Microstructure of iron ores discussed.||Unit in Brockman Iron Formation.||||
27168|Joffre Member|67855|6|Mentioned|p226, 227 fig 3-27|||||Of Brockman Iron Formation||||
27168|Joffre Member|68035|4|Described|p292 Fig 6|Paleoproterozoic|Paleoproterozoic|Hamersley Group, Hamersley Basin.|2465 - 2454 Ma|Of Brockman Iron Formation.||Overlies Whaleback Shale Member. Overlain by Yandicoogina Shale Member.|Banded iron formation.|
27168|Joffre Member|68280|5|Briefly described|p5, p41|Paleoproterozoic|Paleoproterozoic||c. 2454 Ma|Brockman Iron Formation||Overlain by Yandicoogina Shale Member, overlies Whaleback Shale Member|Banded iron formation.|16-JAN-23
27168|Joffre Member|69538|5|Briefly described|p516, p517 Fig.3, p525, p534|||See also p529-531 Figs.9-11, p564 Fig.37, p565, p567-568, p570-571, p583-585. Highly detailed discussion of formation of detrital iron ore deposits.||Unit in Brockman Iron Formation.||Overlies Whaleback Shale Member.||
27168|Joffre Member|69563|6|Mentioned|p691 Fig.1|||||Unit in Brockman Iron Formation.||||
27168|Joffre Member|69745|5|Briefly described|p272, 274, 276-279, 281-282, 288, 290|||Mount Wall Fe deposit area, Hamersley Province. Over 350m thick in drillcores. Has 6 submembers. Has thinner BIF bands and higher content of fine shale partings than Dales Gorge Member.||Brockman Iron Formation.||Is faulted against Woongarra Rhyolite.|Blue to grey banded rocks dominated by chert and magnetite with only smaller amounts of hematite, riebeckite, carbonate and other Fe-silicates.|
27168|Joffre Member|70509|4|Described|p12-16,24-26,28-34|Paleoproterozoic|Paleoproterozoic|Geological province: Hamersley Province; Pilbara Craton. Also referred to as Joffre BIF in text. The largest banded iron formation (BIF) in the world by volume (~4.3 ¿ 10e13 t of iron at the time of deposition; Trendall and Blockley, 2004). Underwent minor folding and basinal uplift; associated low-grade regional metamorphism from burial prehnite-pumpellyite facies to greenschist facies (Smith et al., 1982). SHRIMP U-Pb of 19 zircon grains from interbedded tuffaceous mudrock facies at the top of unit yielded best age estimates of 2454+\-3 Ma, and 2459+\-3 Ma from 6 grains at the base of the unit (Pickard, 2002). Depositional model: Deposited in a large, stable, and clastic-starved, continental platform, with episodic inputs of fine-grained tuffaceous detritus (Gross, 1983; Morris, 1980; Krapez et al., 2003). Possibly a subsiding platform in a backarc setting with tuffaceous material  sourced from subduction-related magmatic arc (Blake and Barley 1992).  Drill core section: DD98SGP001; 355m core section studied for this study. See p15-21 for detailed petrography and mineralogy of the Joffre Member. |~2.45 Ga|Unit of Brockman Iron Formation.||Overlain by Yandicoogina Shale Member. Underlain by Whaleback Shale Member.|Oxide (chert, magnetite, lesser hematite) and silicate-carbonate-oxide (chert, magnetite, riebeckite) BIF, with minor amounts of interbedded stilpnomelane mudrock, stilpnomelane-rich tuffaceous mudrock and calcareous mudrock.|
27168|Joffre Member|71513|6|Mentioned|p79, p87|||Intersected in drillhole Silvergrass.||Brockman Iron Formation||||
27168|Joffre Member|71785|6|Mentioned|p87|||Member Brockman Iron Fm.||||||
27168|Joffre Member|71808|4|Described|viii, p6, p10, p30, p33-p36, p38-p39|||Hamersley Province. Typically forms larger rounded hills than the Dales Gorge Member. Compared with the Dales Gorge Member this unit is less well banded. In the study area the unit is around 200 to 250m thick. Preserved on Wildflower Mountain and the remainder of Packsaddle Range and Fork South. Constituent informally named beds are described in great detail. Referred to as the Joffre Formation p101 mistakenly. See also p43, p45-p47, p53, p67, p81, p86, p88, p101-p102, p117, p135, p202, p214, p228, p234, p242, p244.||Brockman Iron Formation||Overlies the Mount Whaleback Shale Member. Overlain by the Weeli Wolli Formation and Yandicoogina Shale Member.|Chert.|
27168|Joffre Member|72254|5|Briefly described|p360-362, p364-365, App.A p10-11|Siderian|Siderian|Pilbara Craton. Constitutes the largest and best dated BIF unit in the world. Thickness: 400 m. Age range of 2461 +/- 5 to 2445 +/- 5 Ma. Weakly metamorphosed to lower greenschist facies. [Also written as Joffre member in App.A p11].|2461 +/- 5 to 2445 +/- 5 Ma|Brockman Iron Formation, Hamersley Group, Mount Bruce Supergroup|||Banded iron formations with alternating layers of siliceous and ferruginous chemical sediment and occasional thin detrital shales.|
27168|Joffre Member|72493|5|Briefly described|p28, 30, 34|||Hamersley Basin. Contains ""enormous"" amounts of iron in well-banded BIFS with spectacular lateral continuity.",,|2459 +/- 3 Ma - 2454 +/- 3 Ma.|Brockman Iron Formation.||Overlies Whaleback Shale Member. Is overlain by Yandicoogina Shale Member.|BIF, shale.|
27168|Joffre Member|72712|6|Mentioned|p10, p44.|Siderian|Siderian|Easily recognizable despite the tight folding in the core of the Hardey Syncline.|c. 2495 Ma to c. 2460 Ma.|Brockman Iron Formation||Probably overlies Whaleback Shale Member. Probably overlain by Yandicoogina Shale Member.||
27168|Joffre Member|72758|6|Mentioned|p15 Tb.1, p25.|||Occurances of this unit are present over much of north eastern Wyloo.||Brockman Iron Formation|||Banded iron-formation; lacks regular macrobanding and contains thin stilpnomelane bearing shales.|
27168|Joffre Member|73022|6|Mentioned|p2 Fig.1, p3 Fig.2|||||Brockman Iron Formation||Overlies the Whaleback Shale member, underlies the Yandicoogina Shale Member.|Banded iron formation, lesser shale, Fe-chert and minor carbonate.|
27168|Joffre Member|73290|6|Mentioned|p784|||Hamersley Province.||||||
27168|Joffre Member|73538|5|Briefly described|p1-2, p4-7|||Age of ca 2460 Ma was reported by Trendall et al. (2004). [Written as Joffre Iron Formation on p1-2. p5-7].|ca 2460 Ma|Brockman Iron Formation||Underlain by Whaleback Shale. Overlain by Yandicoogina Shale Member.|Iron formation.|
72708|Johansen Monzogranite|64621|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite. Age: 3313-3305 Ma. Biotite monzogranite; medium- to coarse-grained, locally foliated; metamorphosed.||||||16-APR-13
72708|Johansen Monzogranite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Emu Pool Supersuite. c.3303 Ma. Biotite monzogranite; medium- to coarse-grained; locally foliated; metamorphosed.||||||
72708|Johansen Monzogranite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Age derived from sample of coarse grained granodiorite (178075.1.pdf)|3303 +/- 2Ma (SHRIMP)|Emu Pool Supersuite||Intrudes Fig Tree Gneiss, Intruded by Moolyella Monzogranite|Biotite monzogranite; medium- to coarse-grained; locally foliated; metamorphosed|
72708|Johansen Monzogranite|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA 178075 (biotite granodiorite) yielded an interpreted igneous crystallisation age of 3303+\-2 Ma for the granodiorite (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3303 Ma (isotopic)|Unit of Emu Pool Supersuite.||Intrudes into Fig Tree Gneiss. Intruded by Moolyella Monzogranite.|Biotite monzogranite; medium- to coarse-grained; locally foliated; metamorphosed|
72708|Johansen Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
72708|Johansen Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||Max age 3315+/-3 Ma, min 3303+/-2 Ma.|Emu Pool Supersuite|||Biotite monzogranite; medium to coarse grained; locally foliated; metamorphosed.|
25965|Johnny Cake Shale Member|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|Of Duerdin Group.||||||
25965|Johnny Cake Shale Member|28255|5|Briefly described|p76|||Of the Ranford Formation (Duerdin Group).||||||
25965|Johnny Cake Shale Member|32660|6|Mentioned|p223|||||||||
25965|Johnny Cake Shale Member|32728|6|Mentioned|Table 7|||See also Fig.16||||||
25965|Johnny Cake Shale Member|36888|4|Described|p215|||||||||
25965|Johnny Cake Shale Member|36898|5|Briefly described|Table 1|||||||||
25965|Johnny Cake Shale Member|37462|6|Mentioned|p294|||||||||
25965|Johnny Cake Shale Member|37927|6|Mentioned|p511|||||||||
25965|Johnny Cake Shale Member|38157|6|Mentioned|Table X|||||||||
25965|Johnny Cake Shale Member|42047|6|Mentioned|p201|||||||||
25965|Johnny Cake Shale Member|43855|5|Briefly described|Map Legend||Proterozoic|||||||
25965|Johnny Cake Shale Member|44140|5|Briefly described|p301 fig 4-7, p302 Tb.4-2|Neoproterozoic|Neoproterozoic|Of East Kimberley area. 180 m thick. Shortened to Johnny Cake Shale in Fig.4-7.||Ranford Formation||Overlies Jarrad Sandstone Member and ? Moonlight Valley Tillite (apparently conformably).|Green and red banded shale; gypsiferous and dolomitic in part.|07-MAR-18
25965|Johnny Cake Shale Member|44317|4|Described|Table 3, p.7||Adelaidean|||||||
25965|Johnny Cake Shale Member|44318|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
25965|Johnny Cake Shale Member|44868|5|Briefly described|Map Legend||Phanerozoic|||||||
25965|Johnny Cake Shale Member|45047|2|Defined|p92|Adelaidean|Adelaidean|||||||
25965|Johnny Cake Shale Member|45112|6|Mentioned|p36|||||||||
25965|Johnny Cake Shale Member|64104|6|Mentioned|p62 fig.1, p71-73, p75-79|Neoproterozoic|Neoproterozoic|||Unit in Ranford Formation.||Overlies Jarrad Sandstone Member.||
25965|Johnny Cake Shale Member|67484|5|Briefly described|p294-296|Ediacaran|Ediacaran|East Kimberley Region - Donkey Gap section. A new Ediacara-type fossil  Palaeopascichnus has been identified in this unit. If correlation with the early Ediacara formations of SA is accepted, it represents the earliest identifiable member of the Ediacara biota (late Neoproterozoic). The 'Member' is omitted in Tb.1.||Of the Ranford Formation.||Overlies Jarrad Sandstone.|Shale interbedded with dolomitic siltstone.|
25965|Johnny Cake Shale Member|67620|5|Briefly described|p5 Tbl.1|Ediacaran|Ediacaran|East Kimberley region. The rank (Member) is omitted in the Table.||Ranford Formation.||Overlies Jarrad Sandstone Member.||
25965|Johnny Cake Shale Member|68473|6|Mentioned|p531-532|||Up to 42m thick. Microbial mats are present on fine sandstones and siltstones, including erosional remnants, erosional pockets, alpha petees and reticulated ridges.||Ranford Formation||Equivalent to the Throssell Shale.|Dominated by fine sandstone and clay and laminated siltstone, clay and dolomite.|
25965|Johnny Cake Shale Member|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Wolfe Creek Basin||Ranford Formation|||Thin-bedded siltstone and thin- to thick-bedded quartz sandstone, dolomitic quartz sandstone, and dolostone.|31-JUL-15
25965|Johnny Cake Shale Member|69165|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|||Ranford Formation|||Thin-bedded siltstone and thin to thick bedded quartz sandstone, dolomitic quartz sandstone and dolostone.|
25965|Johnny Cake Shale Member|69634|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1.|635-541 Ma (Inferred)|Unit of Ranford Formation.|||Thin-bedded siltstone and thin- to thick-bedded quartz sandstone, dolomitic quartz sandstone, and dolostone|
25965|Johnny Cake Shale Member|70154|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran||541-635 Ma|Duerdin Group|||Thin bedded siltstone and thin to thick bedded quartz sandstone, dolomitic quartz sandstone and dolostone.|
25965|Johnny Cake Shale Member|71267|5|Briefly described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma).|635-541 Ma (inferred)|Unit of Ranford Formation.|||Thin-bedded siltstone and thin- to thick-bedded quartz sandstone, dolomitic quartz sandstone, and dolostone|
31760|Johnson Cairn Formation|7471|5|Briefly described|p8, Map legend|Proterozoic|Proterozoic|Yerrida Basin. Terrigenous, sedimentary. Mis-spelt as Johnstone in map legend.||Of the Windplain Subgroup (Yerrida Group).||Overlies Juderina Formation.|Siltstone and thin-bedded dolomite.|
31760|Johnson Cairn Formation|12099|4|Described|p677-8, 680-1, 683 Figs.2, 4, 5, 6|Statherian|Paleoproterozoic|Up to 1250m thick.||Unit in Windplain Subgroup.||Overlies Juderina Formation. Conformably overlain by Thaduna Formation.|Succession of varicoloured iron-rich shale, with graded silty layers and thin dolomite bands.|04-MAR-13
31760|Johnson Cairn Formation|22501|6|Mentioned|p117 Fig. 3|||in the Yerrida Province||||||
31760|Johnson Cairn Formation|22694|5|Briefly described|p7|||||||||
31760|Johnson Cairn Formation|22940|4|Described|Fig.1 p3|||See also Table 2 p12. of Windplain Subgroup, Yerrida Group.||||||
31760|Johnson Cairn Formation|23581|5|Briefly described|Map legend|||Of the Windplain Subgroup in the Yerrida Group in the Yerrida Basin||||||
31760|Johnson Cairn Formation|23589|5|Briefly described|p15|||Of Windplain Subgroup. Underlying unit Juderina Formation.||||||
31760|Johnson Cairn Formation|23593|4|Described|p9|||Of Windplain Subgroup. Overlying unit Thaduna Formation. Underlying unit Juderina Formation. Geological Province: Yerrida Basin.||||||
31760|Johnson Cairn Formation|23597|4|Described|p10|||Of Windplain Subgroup. Overlying unit Thaduna Formation. Underlying unit Juderina Formation. Yerrida Basin. Max. thickness: ~1250 m.||||||
31760|Johnson Cairn Formation|23600|4|Described|p8|Proterozoic|Proterozoic|Previously Johnson Cairn Shale. Of Windplain Subgroup. Overlying unit Thaduna Formation. Underlying unit Juderina Formation. Geological Province: Yerrida Basin. Max. thickness: 250 m.||||||26-FEB-13
31760|Johnson Cairn Formation|23744|4|Described|p11|Paleoproterozoic|Paleoproterozoic|See also page 10 table 1. Of Windplain Subgroup. Geological Province: Yerrida Basin.||||||07-NOV-08
31760|Johnson Cairn Formation|23747|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|See also page 4 table 1. Of Windplain Subgroup. Geological Province: Yerrida Basin.||||||07-NOV-08
31760|Johnson Cairn Formation|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Windplain Subgroup. Geological Province: Yerrida Basin.||||||
31760|Johnson Cairn Formation|23749|4|Described|p7|Proterozoic|Proterozoic|Formerly Johnson Cairn Shale. Of Windplain Subgroup. Geological Province: Yerrida Basin.||||||
31760|Johnson Cairn Formation|23750|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Windplain Subgroup. Geological Province: Yerrida Basin.||||||
31760|Johnson Cairn Formation|23865|5|Briefly described|p170 Fig.1|||Of Windplain Subgoup. Geological Province: Yerrida Basin.||||||
31760|Johnson Cairn Formation|23890|4|Described|p20|Paleoproterozoic|Paleoproterozoic|Of Yerrida Group. Geological Province: Yerrida Basin.||||||07-NOV-08
31760|Johnson Cairn Formation|24021|3|Fully described|p12|Paleoproterozoic|Paleoproterozoic|Parent: Windplain Subgroup.   Geological Province: Yerrida Basin||||||20-JAN-10
31760|Johnson Cairn Formation|24028|5|Briefly described|p289|Paleoproterozoic|Paleoproterozoic|Of Windplain Subgroup.  Geological Province: Yerrida Basin.||||||07-NOV-08
31760|Johnson Cairn Formation|24535|5|Briefly described|p22, 23|Paleoproterozoic|Paleoproterozoic|Of the Windplain Group. Geological Province: Yerrida Basin.||||||26-NOV-13
31760|Johnson Cairn Formation|43831|5|Briefly described|Map Legend||Paleoproterozoic|Yerrida Basin.||||||07-NOV-08
31760|Johnson Cairn Formation|43836|5|Briefly described|Map Legend||Proterozoic|of Windplain Subgroup. Yerrida Basin.||||||
31760|Johnson Cairn Formation|43837|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Windplain Subgroup (Yerrida Group).  Argillaceous siltstone and thin-bedded dolomite, minor lithic and quartz sandstone.||||||18-MAY-04
31760|Johnson Cairn Formation|44204|5|Briefly described|Map Legend||Proterozoic|||||||
31760|Johnson Cairn Formation|44830|5|Briefly described|Map Legend||Proterozoic|||||||
31760|Johnson Cairn Formation|49893|4|Described|p13|Proterozoic|Proterozoic|Of the Windplain Subgroup. Geological Province: Yerrida Basin. Conformably overlies Juderina Formation. Conformably overlain by Thaduna Formation. Supersedes Johnson Cairn Shale, Gee (1987). Max. thickness: 1250m. See also p2 Fig.1.||||||
31760|Johnson Cairn Formation|49896|5|Briefly described|p3 Tb. 2|||Of Occhipinti et al (1997). Supersedes Johnson Cairn Shale. Now of the Windplain Subgroup (Yerrida Group). ||||||
31760|Johnson Cairn Formation|49912|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Yerrida Group.  Geological Province: Yerrida Basin.||||||
31760|Johnson Cairn Formation|50222|5|Briefly described|p320 Fig. 3, p321|Paleoproterozoic|Paleoproterozoic|Of the Windplain Group.  Iron-rich shales with graded silty layers and thin dolomite bands.  Disconformably overlies Juderina Formation; disconformably overlain by Thaduna Formation (Mooloogool Group).  Max. thickness: 1200m.  Geol. Prov: Yerrida Basin.||||||07-NOV-08
31760|Johnson Cairn Formation|61269|6|Mentioned|p87 Fig.2|||||||||
31760|Johnson Cairn Formation|61271|6|Mentioned|p105 Fig.1|||Of the Windplain Group.||||||
31760|Johnson Cairn Formation|62289|4|Described|plate 1, p3 Fig. 1, p7-8, p11-12, p16-17|Palaeoproterozoic|Palaeoproterozoic|Supersedes Johnson Cairn Shale (Occhipinti et al. 1997); conformable on Juderina Formation and  interdigitates with Killara Formation; conformably overlain by Thaduna Formation; fault contact with Bryah Group; type area given; thickness: up to 1250 m; varicoloured iron-rich shale, with graded silty layers and thin dolomite bands.||||||
31760|Johnson Cairn Formation|62353|5|Briefly described|map legend|Proterozoic|Proterozoic|Geol. Prov: Yerrida Basin.||Of Windplain Subgroup, Yerrida Group.||Underlies Doolgunna Formation.|Shale and siltstone, partly carbonaceous and dolomitic; minor quartz arenite, wacke, dolomite lenses, and disseminated lenses of iron-rich concretions.|14-APR-11
31760|Johnson Cairn Formation|63866|5|Briefly described|p165|||Yerrida Basin.||Windplain Subgroup|||Iron-rich shales.|
31760|Johnson Cairn Formation|64580|4|Described|map legend||Paleoproterozoic|Of Windplain Group. Shale and siltstone; minor quartz arenite; feldspathic sandstone; and thin-bedded dolomite and marl.||||||15-DEC-08
31760|Johnson Cairn Formation|65408|4|Described|pp82-83.|Paleoproterozoic|Paleoproterozoic|Relatively deeper water facies of the sag-basin succession.||Upper unit in Windplain Subgroup.||Transitionally overlies Juderina Formation.|Siltstone, shale, carbonate, minor lithic wacke.|
31760|Johnson Cairn Formation|65419|1|Redefined|p4 Fig.1, p7, p10 Fig.3, p15, pp17-18.|Paleoproterozoic|Paleoproterozoic|Originally the Johnson Cairn Shale (Gee, 1987; Gee and Grey 1993); name changed to reflect the heterolithic nature of the strata. Named after Johnson Cairn. Reference area is 13 km NE of Thaduna. Some areas to the west of the Great Northern Highway on the Doolgunna 1:100 000 sheet, previously assigned to this unit, are now assigned to the Peak Hill Schist. Includes poorly outcropping argillite overlying the Bubble Well Member in the Finlayson Range in the southeast Glengarry Basin. Thickness to 1200 m. ||Unit in Windplain Subgroup.||Conformably and transitionally overlies Bubble Well Member. Intercalated with Killara Formation. Is overlain transitionally/conformably by Thaduna Formation and disconformably by Doolgunna Formation.|Laminated varicoloured, iron-rich argillite and graded silty layers and carbonate beds; thin (10 cm) purplish laminated micritic dolomite and white pisolitic dolomite-magnesite rock weathering to flaky, chocolate-coloured rubble.|
31760|Johnson Cairn Formation|65472|5|Briefly described|p3 Fig.2|||Thickness: 500-1200 m. Yerrida Basin.||Of Windplain Group.||||24-SEP-15
31760|Johnson Cairn Formation|65896|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Topmost unit in Yerrida Group, Yerrida Basin. Shale and slate.||||||
31760|Johnson Cairn Formation|65913|5|Briefly described|p2 Fig.1, p6, p24.|Paleoproterozoic|Paleoproterozoic|Black argillites are locally anomalous in Cu (up to 2800 ppm), Zn and Hg.||Unit in Windplain Subgroup.||Overlies Juderina Formation. Is overlain by Doolgunna, Thaduna and Killara Formations.|Purple- to cream-coloured, finely laminated siltstones and shales; minor carbonate, lithic wacke.|
31760|Johnson Cairn Formation|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic|Yerrida Basin||Windplain Group|||Shale and siltstone; minor quartz arenite; feldspathic sandstone; and thin-bedded dolomite and marl|
31760|Johnson Cairn Formation|69003|5|Briefly described|p10, p12|||Yerrida Basin. 500-1200m thick.||Windplain Group.||Conformably overlies Juderina Formation. Is overlain unconformably by Killara and Thaduna Formations.|A thick sequence of shales.|
31760|Johnson Cairn Formation|69152|4|Described|500k_geologyp08_lut||Paleoproterozoic|||Windplain Group|||Shale and siltstone; minor quartz arenite; feldspathic sandstone; and thin-bedded dolomite and marl.|06-AUG-15
31760|Johnson Cairn Formation|69166|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|||Windplain Group|||Shale and siltstone; minor quartz arenite; feldspathic sandstone; and thin-bedded dolomite and marl.|
31760|Johnson Cairn Formation|69583|5|Briefly described|Plate 2|Proterozoic|Proterozoic|Yerrida Basin.||Windplain Group.|||Quartz sandstone; local sandstone, shale, siltstone, chert breccia, and conglomerate.|
31760|Johnson Cairn Formation|69596|5|Briefly described|p9-10, p17|||Yerrida, Bryah Basins.||Windplain Group.|||Graphitic and pyritic shales.|
31760|Johnson Cairn Formation|70136|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Yerrida Basin.||Windplain Group.|||Shale and siltstone; minor quartz arenite; feldspathic sandstone; and thin-bedded dolomite and marl.|
31760|Johnson Cairn Formation|70153|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic||2500 - 1600 Ma (inferred).|Windplain Group|||Shale and siltstone; minor quartz arenite, feldspathic sandstone, and thin-bedded dolomite and marl.|
31760|Johnson Cairn Formation|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_interpgeop_lut.csv, West Australian Craton, Yerrida Basin|2500-1600 Ma|Windplain Group|||Shale and siltstone; minor quartz arenite, feldspathic sandstone, and thin-bedded dolomite and marl.|
31760|Johnson Cairn Formation|70796|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|Yerrida Basin, Capricorn Orogen. Misspelt as the Johnstone Cairn Formation in glengarry_100k_geologyp_lut.csv, glengarry_500k_interpgeop_lut.csv, site_lithology.csv, Glengarry100_2645_stratig.pdf.|ca 25001600 Ma (inferred)|Windplain Group|||Shale and siltstone; minor quartz arenite, feldspathic sandstone, and thinbedded dolomite and marl.|
31760|Johnson Cairn Formation|70804|5|Briefly described|p2, p37, plate 1|||Replaces the obsolete Johnson Cairn Shale.||Windplain Subgroup||||
31760|Johnson Cairn Formation|70814|6|Mentioned|p48|||||||||
31760|Johnson Cairn Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, shale, sandstone, crystalline dolostone/dolomite|
31760|Johnson Cairn Formation|71269|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen, West Australian Craton. Of Yerrida Basin. Events: Capricorn Orogeny (1817-1772 Ma).  See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, glengarry_100k_geologyp_lut.csv, glengarry_500k_interpgeop_lut.csv.|2170-1600 Ma (inferred)|Unit of Windplain Group.|||Shale and siltstone; minor quartz arenite, feldspathic sandstone, and thin-bedded dolomite and marl|
31760|Johnson Cairn Formation|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen. Of Yerrida Basin. Events: Capricorn Orogeny (1817 - 1772 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv.|2170-1600 Ma (inferred)|Unit of Windplain Group.|||Shale and siltstone; minor quartz arenite, feldspathic sandstone, and thin-bedded dolomite and marl|
31760|Johnson Cairn Formation|71484|4|Described|p124-126,128-129,133-134,139|||Geological province: Of Yerrida Basin. Regional mapping suggests that contact with underlying Juderina Formation is gradational, however contact sharp/disconformably as intersected in drillhole TDH001, suggesting a fault contact, possibly a slipped unconformity.||Unit of Windplain Group.||Overlain by, and interfingers with Killara Formation. Underlain by Juderina Formation.|Shale and siltstone; minor quartz arenite, feldspathic sandstone, thin-bedded dolomite and marl.|30-AUG-19
31760|Johnson Cairn Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Yerrida Basin.||Windplain Group|||Shale and siltstone; minor quartz arenite, feldspathic sandstone, and thin-bedded dolomite and marl.|
25092|Johnson Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p223|Eocene|Paleocene|In figure, Fm = Formation. Geological Province: Bonaparte Basin. Interbedded carbonate lithologies.||||||01-MAR-10
25092|Johnson Formation|22663|5|Briefly described|AC97 1-4 Fig.4||Paleocene|Woodbine Group.||||||01-MAR-10
25092|Johnson Formation|24171|5|Briefly described|p722 Fig. 3|Tertiary|Tertiary|Geological Province : Vulcan Sub-Basin||||||01-MAR-10
25092|Johnson Formation|24218|5|Briefly described|p850|Paleocene|Paleocene|Geological Province: Bonaparte Basin.||||||
25092|Johnson Formation|42053|5|Briefly described|Fig.2 P29|||||||||01-MAR-10
25092|Johnson Formation|42066|5|Briefly described|Fig.3 P199|||||||||01-MAR-10
25092|Johnson Formation|43826|6|Mentioned|Fig.2,p163||Paleogene|||||||01-MAR-10
25092|Johnson Formation|60385|4|Described|p272 Fig 3|Danian|Maastrichtian|Browse Basin. |||||Limestone, minor sandstone.|
25092|Johnson Formation|60634|6|Mentioned|p1168 Fig.3. |Palaeocene|Palaeocene|||Unit in Bathurst Island Group.||Overlies Puffin and Borde Formations. Is overlain by Grebe Formation.||
25092|Johnson Formation|61548|6|Mentioned|p480 Fig.3|Paleocene|Paleocene|Northern Bonaparte Basin.||||||
25092|Johnson Formation|61550|6|Mentioned|p495 Fig.2. |Paleocene|Paleocene|||Basal unit in Woodbine Group.||Overlies Puffin Formation. Is overlain by Grebe Formation.||
25092|Johnson Formation|62837|5|Briefly described|Stratigraphic columns|Paleocene|Paleocene|Age: 65-~56Ma. Geological Province: Western Bonaparte Basin and Northern Bonaparte Basin.||||||01-MAR-10
25092|Johnson Formation|64695|5|Briefly described|p262 Fig.8|Palaeocene|Palaeocene|Northern Bonaparte Basin.||||Overlies Wangarlu and Turnstone Formations.||
25092|Johnson Formation|64697|5|Briefly described|p84 Fig.2 |Paleocene|Palaeocene|||||||
25092|Johnson Formation|65680|6|Mentioned|p709 Fig.2.|Thanetian||||||Is overlain by Hibernia Formation.||
25092|Johnson Formation|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Eocene|Paleocene|Unit in Woodbine Group. Underlies the Grebe Formation, overlies the Puffin Formation. Mount Ashmore Dome. Limestone dominated with claystone at base.||||||
25092|Johnson Formation|68223|6|Mentioned|p178 Fig.3, p179 Fig.4|Paleocene|Paleocene|||||||
25092|Johnson Formation|69452|5|Briefly described|p36:15, 22|Paleogene|Paleogene|Bonaparte Basin.||Woodbine Group.||||12-JUL-16
25092|Johnson Formation|69673|6|Mentioned|p174|||||||||
25092|Johnson Formation|70061|5|Briefly described|Regional geology; Figs.6-7, p12|Eocene|Paleocene|See also Sahul: Fig.2, p2. Vulcan: Fig.2, p2-3. Carbonates of this unit seal Wangarlu and Puffin Formations exploration targets. Potential oil reservoir in Vulcan Sub-basin.||Woodbine Group.||Overlies Turnstone and Puffin Formations. Is overlain by Hibernia Formation.||12-JUL-16
25092|Johnson Formation|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Paleocene|Paleocene|See also Northern: Fig.2. Brecknoff-Scott Reef Trend, Browse Basin.||Woodbine Group.||Overlies Puffin Formation. Equivalent to Bassett Formation.||12-JUL-16
25093|Jones Creek Conglomerate|7471|6|Mentioned|p7, Map legend|Archean|Archean|Agnew-Wiluna belt. The granite clats indicate granitoid intrusions as pre-greenstone.|||||Metaconglomerate. Shows a variety of textures and compositions. Contains granite clasts.|
25093|Jones Creek Conglomerate|22450|6|Mentioned|p21||Archean|Yilgarn Craton||||||07-NOV-08
25093|Jones Creek Conglomerate|23209|6|Mentioned|p10 Fig.10|||||||||
25093|Jones Creek Conglomerate|23281|6|Mentioned|p5|||||||||
25093|Jones Creek Conglomerate|23586|5|Briefly described|p7|||||||||
25093|Jones Creek Conglomerate|23587|6|Mentioned|p8|||||||||
25093|Jones Creek Conglomerate|23595|4|Described|p14|Archean|Archean|Age: 2632+/-13 Ma (SHRIMP U-Pb zircon). Geological Province: Yilgarn Craton||||||07-NOV-08
25093|Jones Creek Conglomerate|23611|5|Briefly described|p11|Archean|Archean|Age: 2667+/-6 Ma (SHRIMP U-Pb). See also page 31 Appendix 1. Geological Province: Yilgarn Craton. Max. thickness: 1000 m.||||||07-NOV-08
25093|Jones Creek Conglomerate|23759|6|Mentioned|p7|||||||||
25093|Jones Creek Conglomerate|23782|5|Briefly described|p29 Fig. 21|||Geological Province: Yilgarn Craton.||||||
25093|Jones Creek Conglomerate|23786|5|Briefly described|p28|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
25093|Jones Creek Conglomerate|24135|3|Fully described|p18|Archean|Archean|||||||07-NOV-08
25093|Jones Creek Conglomerate|24174|4|Described|p39, p5 Fig. 2|||Geological Province: Eastern Goldfields.||||||
25093|Jones Creek Conglomerate|24196|6|Mentioned|p68|||See also Jones Creek conglomerate.||||||
25093|Jones Creek Conglomerate|24494|5|Briefly described|p13, p39 App.1|Archean|Archean|Known locally as the "Scotty Creek Formation". Age: 2667 +/- 6 Ma (U-Pb; Nelson, 2000)||||||07-NOV-08
25093|Jones Creek Conglomerate|29784|6|Mentioned|p27|||||||||
25093|Jones Creek Conglomerate|30631|4|Described|p252|||Archaean age. See also p253.||||||30-SEP-08
25093|Jones Creek Conglomerate|32010|6|Mentioned|p160|||||||||
25093|Jones Creek Conglomerate|32011|3|Fully described|p143|||||||||
25093|Jones Creek Conglomerate|32907|6|Mentioned|Fig.1|||||||||
25093|Jones Creek Conglomerate|33558|5|Briefly described|p156|||Stratigraphy||||||
25093|Jones Creek Conglomerate|34885|6|Mentioned|p114|||||||||
25093|Jones Creek Conglomerate|35113|6|Mentioned|Fig.5|||See also P49||||||
25093|Jones Creek Conglomerate|37633|5|Briefly described|Table 63|||||||||
25093|Jones Creek Conglomerate|38459|6|Mentioned|p1551|||||||||
25093|Jones Creek Conglomerate|40775|4|Described|p500|||||||||
25093|Jones Creek Conglomerate|43162|6|Mentioned|34|||||||||
25093|Jones Creek Conglomerate|43288|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
25093|Jones Creek Conglomerate|44149|5|Briefly described|p81 Tb.2-8, p91,p93,p94 fig 2-97,p109|Archean|Archean||||||Sequence of conglomerate and arkosic sandstone.|
25093|Jones Creek Conglomerate|44924|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
25093|Jones Creek Conglomerate|60416|5|Briefly described|p5, p16, p17-18|||Comprises granitoid-clast conglomerate and sandstone with some interbedded siltstone.  See also p27 Tb. 1, p33.||||||
25093|Jones Creek Conglomerate|60514|6|Mentioned|p113|Archean|Archean|Geological Province: Yilgarn Craton. Includes a mix of felsic, mafic and ultramafic volcanic rocks.||||||07-FEB-11
25093|Jones Creek Conglomerate|60623|5|Briefly described|p33|Archean|Archean|Fluvial unit equivalent to Merougil Formation.||||||07-NOV-08
25093|Jones Creek Conglomerate|60630|5|Briefly described|p113|||Overlies quartz-feldspar porphyry intrusion||||||
25093|Jones Creek Conglomerate|63711|5|Briefly described|p849 Fig. 2|||Geological Province: in the Mount Keith domain of the Agnew-Wiluna Greenstone Belt of Western Australia.||||||15-JAN-08
25093|Jones Creek Conglomerate|63712|6|Mentioned|p839 Fig. 7|||||||||
25093|Jones Creek Conglomerate|64586|5|Briefly described|Map legend|Archean|Archean|Conglomerate and sandstone with granitoid clasts and matrix dominating, metamorphosed. Arkosic arenite, fine- to medium-grained, rare pebbles - metamorphosed. Conglomerate and sandstone with mafic matrix dominating - metamorphosed.||||||24-APR-17
25093|Jones Creek Conglomerate|64633|6|Mentioned|p6 Fig.4, p8.|||?Kurnalpi Terrane or part of later basin?.|<2665 +/- 5 Ma (Krapez et al. 2000).|||||24-APR-17
25093|Jones Creek Conglomerate|65200|5|Briefly described|Map legend|Archean|Archean|Metamorphosed arkosic sandstone and siltstone of the Yilgarn Craton.||||||24-NOV-09
25093|Jones Creek Conglomerate|65264|5|Briefly described|p10, p21, p51 Appdx. 1|Archean|Archean|Max.thickness:1000m. Geol.prov: Agnew-Wiluna greenstone belt. Dominant rock type is variably deformed polymictic conglomerate - detailed lithological descriptions included.||||||07-FEB-11
25093|Jones Creek Conglomerate|66192|6|Mentioned|p545 Fig.2|||||||Overlies Monument Ultramafic Unit.||09-MAR-12
25093|Jones Creek Conglomerate|66880|6|Mentioned|p8 Fig.2. |Archean|Archean|Wiluna Domain.|2665 +/- 5 Ma (Krapez et al. 2000).|||||
25093|Jones Creek Conglomerate|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton. U/Pb SHRIMP age data from geochron file 118937.1.pdf, 118937.2.pdf (1997, 2000).|max deposit age: 2667+/-6 Ma||Includes 4 unnamed subunits.||Polymictic conglomerate; conglomerate and sandstone; dominantly granitic clasts; conglomerate and sandstone with mafic and granitic clasts and dominantly mafic matrix; arkosic sandstone, fine to medium grained; all  metamorphosed.|06-AUG-15
25093|Jones Creek Conglomerate|69414|6|Mentioned|p88, 90, 102|Archean|Archean|Agnew-Wiluna Greenstone belt, Yilgarn Craton.|2667 +/- 6 Ma (MDA: Nelson, 1997).||||Rounded granitic clasts in an arkosic or mafic matrix. Includes metasandstone.|
25093|Jones Creek Conglomerate|69583|5|Briefly described|p39; Plate 2|Archean|Archean|Has an age similar to the Scotty Creek Formation to the south.|c.2662 Ma.|||Correlated with Merougil Group.|Metamorphosed conglomerate and sandstone.|
25093|Jones Creek Conglomerate|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|See also 500k_interpgeop14_lut.csv. Age derived from metasandstone sample (118937.1.pdf) and constrains maximum date for deposition of sandstone protolith. Another age range given is 2665 +/- 5 Ma (isotopic) - 2640 Ma (inferred).|2667 Ma +/- 6 Ma (SHRIMP)||||Polymictic conglomerate; metamorphosed. Conglomerate and sandstone with mafic and granitic clasts; fine to medium grained arkosic sandstone.|
25093|Jones Creek Conglomerate|70275|5|Briefly described|p471-472, 476, 478, 496|||Central Mt. Keith portion of the Agnew-Wiluna Belt, Kalgoorlie Terrane, Yilgarn Craton. Deposited in synorogenic basins. Mis-spelled as James Creek Conglomerate on p496.|2665 +/- 5 Ma.|||Overlies Mount White Formation.|Siliciclastic sequences.|
25093|Jones Creek Conglomerate|70276|6|Mentioned|p784|||Agnew-Wiluna greenstone belt, Yilgarn Craton.|2665 +/- 5 Ma.|||||
25093|Jones Creek Conglomerate|70773|6|Mentioned|p60|||||||||
25093|Jones Creek Conglomerate|70826|6|Mentioned|p9|Neoarchean|Neoarchean|||||||13-MAY-20
25093|Jones Creek Conglomerate|71212|5|Briefly described|p1, p69, p89, p143|Neoarchean|Neoarchean|Yilgarn Craton. Ages are SHRIMP U-Pb zircon dates likely are the crystallization ages of the granitic source rock from which the conglomerate is formed and thus represent the maximum depositional age of the Jones Creek Conglomerate. An older age of approximately 2816 +/- 13 Ma (Krapez et al, 2000) likely represents xenocrysts of older crustal material derived during petrogenesis and emplacement of the granite protolith that later formed this unit. Another age of 2665 +/- 5 Ma is given (Krapez et al, 2000). See also p239, p240, p241, p242, p245, p250.|2667+/- 6 Ma (Nelson, 2000) |||Unconformably overlies the Kathleen Valley Gabbro and the Mount Goode Basalt. Probable lateral equivalent of the Scotty Creek Metasediments.|Epiclastic conglomerate derived from a single granitic source.|
25093|Jones Creek Conglomerate|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma); Yilgarn Craton events (4000 - 2600 Ma). See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv. Sample GSWA 118937 (metamorphosed feldspathic sedimentary rock) yielded weighted mean 207Pb/206Pb date of 2667+\-6 Ma, interpreted to be maximum depositional age of the sandstone protolith.|2665+\-5 Ma; 2640 Ma (inferred)||||Polymictic conglomerate and arkosic sandstone with mafic and granitic clasts and dominantly mafic or quartzofeldpsathic matrix; metamorphosed|
25093|Jones Creek Conglomerate|71310|4|Described|p765, p768 Fig.2, p774-778, p780-788|||Previously the Scotty Creek Formation (Aoukar and Whelan, 1990). Western limb of the Lawlers antiform; folding and deformation described in detail. Hosts the Waroonga, New Holland and Genesis gold deposits (described in some detail). Some clasts sourced from Kathleen Valley Gabbro. Less than 2.6km thick.|2664 +/- 5 Ma (maximum depositional age).|||Unconformably overlies Kathleen Valley Gabbro.|Basal conglomerate and overlying cross-bedded sandstone.|
25093|Jones Creek Conglomerate|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||Max age 2665+/-5 Ma, min ~2640 Ma.||||Conglomerate and sandstone; metamorphosed.|
25093|Jones Creek Conglomerate|72049|5|Briefly described|p256, p259|||Geochronology analyses, results, and interpretation are discussed in detail.||Kurrawang Group||||
25093|Jones Creek Conglomerate|73238|6|Mentioned|p12||||2665 +/- 5 Ma (Krapez et al., 2000).|||||
73589|Jones Well Granodiorite|63441|5|Briefly described|p11 Tb. 2, p37|Archean|Archean|Part of the Indee Suite (Sisters Supersuite). Geological province: Mallina Basin/Pilbara Craton. On the SATIRIST map sheet.||||||07-FEB-11
73589|Jones Well Granodiorite|70775|6|Mentioned|p65|||||Indee Suite||||
39504|Joorina Granodiorite|63417|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite.  Age: 3321-3304Ma. Geological Province: Pilbara Craton. Biotite granodiorite, locally includes tonailte and monzogranite; medium- to coarse-grained; locally seriate and porphyritic; weakly to mod. foliated; metamorphosed.||||||07-NOV-08
39504|Joorina Granodiorite|63441|5|Briefly described|p8 Tb. 2|Archean|Archean|Of Emu Pool Supersuite. Replaces Boodallana Suite. Ages: from 3321+/-6Ma to 3304+/-10Ma. Geological province: Pilbara Craton.||||||07-FEB-11
39504|Joorina Granodiorite|64621|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite. Age: 3321-3304Ma. Biotite granodiorite; local tonalite and monzogranite; locally porphyritic; variably foliated; metamorphosed.||||||07-NOV-08
39504|Joorina Granodiorite|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.|c.3304 Ma (Nelson 2002).|Of Mount Edgar Granitoid Complex.|||Biotite granodiorite, tonalite and monzogranite; fine- to coarse-grained, locally seriate and porphyritic; weakly to moderately foliated; mafic xenoliths.|
39504|Joorina Granodiorite|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|3321 - 3304 Ma (Williams and Collins 1990).|Of Emu Pool Supersuite.|||Biotite granodiorite, local tonalite and monzogranite; medium- to coarse-grained, locally porphyritic; weakly to moderately foliated; mafic xenoliths; weakly metamorphosed.|
39504|Joorina Granodiorite|65827|2|Defined|p6 Tb.2, p13 Tb.4, p20, p23, p58|Paleoarchean|Paleoarchean|New name; after Joorina Well. 3321 +/- 6 Ma (SHRIMP U-Pb zircon; Nelson 2000) to 3304 +/- 10 Ma (Williams and Collins 1990); possibly a number of discrete bodies.||Of Emu Pool Supersuite.|Includes the former Boodallana Suite.|Intruded by Bishop Creek Monzogranite, Kennell Granodiorite; intrudes Fig Tree Gneiss; intruded by rocks correlated with Warrawoona Group.|Multiply deformed, foliated, seriate to locally porphyritic, biotite(-hornblende) tonalite, granodiorite, and monzogranite; mafic schlieren and biotite clots are common.|21-MAY-14
39504|Joorina Granodiorite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Emu Pool Supersuite. 3321-3304 Ma. Biotite granodiorite; local tonalite and monzogranite; locally porphyritic; variably foliated; metamorphosed.||||||15-APR-13
39504|Joorina Granodiorite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Emu Pool Supersuite|||Biotite granodiorite; local tonalite and monzogranite; locally porphyritic; variably foliated; metamorphosed|
39504|Joorina Granodiorite|69566|6|Mentioned|p236|||Mount Edgar Granitoid Complex, East Pilbara Granite-Greenstone Terrane.||Emu Pool Supersuite.||||
39504|Joorina Granodiorite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3321-3304 Ma (isotopic)|Unit of Emu Pool Supersuite.|||Biotite granodiorite; local tonalite and monzogranite; locally porphyritic; variably foliated; metamorphosed|
39504|Joorina Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite, tonalite, monzogranite|
39504|Joorina Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||Max age 3321+/-6 Ma, 3304+/- 10 Ma|Emu Pool Supersuite|||Biotite granodiorite; local tonalite and monzogranite; locally porphyritic; variably foliated; metamorphosed.|
31961|Joy Helen Granite|24197|6|Mentioned|p71 Tb. 7.1|||Of the Chararoo Supersuite.||||||07-FEB-11
31961|Joy Helen Granite|50425|5|Briefly described|p1.3, 3.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Province. Of the Chararoo Supersuite.||||||07-NOV-08
23674|Judy Member|42615|4|Described|p30|||of Athol Formation. Reserved.||||||
22039|Juglah Monzogranite|43075|6|Mentioned|p10|||||||||
22039|Juglah Monzogranite|64775|6|Mentioned|p13-1|||||||||
22039|Juglah Monzogranite|70087|6|Mentioned|p215|Archean|Archean|Forms part of the core of the Bulong Dome, Mount Monger region, Eastern Goldfields Superterrane.|2635 +/- 4 Ma (Dunphy et al., 2003).|||||
22047|Junda Microgranite|22496|5|Briefly described|p7|Orosirian|Orosirian|1913 +/- 5 Ma||||||
22047|Junda Microgranite|22754|5|Briefly described|p6, p8|Paleoproterozoic|Paleoproterozoic|Of the Sophie Downs suite.  Age: c. 1912Ma.||||||09-DEC-08
22047|Junda Microgranite|23599|4|Described|p8|Paleoproterozoic|Paleoproterozoic|Age: c.1910-1920 Ma. See also page 5 Table 1. Overlying unit Saunders Creek Formation.||||||07-NOV-08
22047|Junda Microgranite|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Partly recrystallised fine-grained leucocratic monzogranite. Age: c.1910Ma. In the Lamboo Complex (eastern zone).||||||26-NOV-15
22047|Junda Microgranite|44693|5|Briefly described|Map Legend||Proterozoic|||||||
22047|Junda Microgranite|50437|5|Briefly described|p1.6, 5.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Sophie Downs Suite. Age: 1913 +/- 5Ma (Shrimp).||||||07-NOV-08
22047|Junda Microgranite|63866|5|Briefly described|p128-p129, p138|Orosirian|Orosirian|Eastern Zone, Halls Creek Orogen.|c. 1912-1907 Ma|||||
22047|Junda Microgranite|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Partly recrystallized; leucocratic monzogranite and garnet-muscovite granite.||||||09-DEC-08
22047|Junda Microgranite|68656|5|Briefly described|GEOL_LUT_CSV/500k_geologyp08_lut|Paleoproterozoic|Paleoproterozoic|Described with Esaw Monzogranite.|||||Partly recrystallized; leucocratic monzogranite and garnet-muscovite granite.|
22047|Junda Microgranite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Data from OZCHRON1. Comment: 'Fifteen concordant data points fit this 207/206 age to within experimental error. The age is the magmatic crystallisation event, preceding deposition of the Halls Creek Group.'|crystallisation age: 1913+/-5 Ma U/Pb SHRIMP|Sophie Downs Suite|||Fine-grained, leucocratic biotite metamonzogranite.|31-JUL-15
22047|Junda Microgranite|69165|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv. |1913 Ma||||Partly recrystallized; leucocratic monzogranite and garnet muscovite granite.|
22047|Junda Microgranite|69587|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Partly recrystallized; leucocratic monzogranite and garnet-muscovite granite|
22047|Junda Microgranite|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|1913-1913 Ma (Isotopic)|Unit of Sophie Downs Suite.|||Fine-grained, leucocratic biotite metamonzogranite|
22047|Junda Microgranite|70154|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv.|1913 Ma||||Fine grained, leucocratic biotite metamonzogranite.|
22047|Junda Microgranite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1911+\5 Ma (isotopic)|Unit of Sophie Downs Suite.|||Fine-grained, leucocratic biotite metamonzogranite, partly recrystallised|
22047|Junda Microgranite|71397|4|Described|p8,10,30-32|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen. Crops out in the cores of a series of structural domes in the southeast on DOCKRELL map sheet. Tyler et al. (1998) reported a SHRIMP U-Pb age of 1913+\-8 Ma. Zircon U-Pb geochronological analysis of the sample from Tyler et al. (1998) yielded a weighted mean 207Pb*/206Pb* date of 1911+\-5 Ma, interpreted as the age of magmatic crystallisation.|1911+\-5 Ma|Unit of Sophie Downs Suite.|||Foliated and recrystallized, fine-grained leucocratic monzogranite.|
22047|Junda Microgranite|72437|5|Briefly described|p7, p51|Palaeoproterozoic|Palaeoproterozoic|Analysed (once) in this study.|c. 1910 Ma|Sophie Downs suite|||Foliated fine-grained biotite monzogranite.|
35677|Jundee Basalt|23149|5|Briefly described|p101 Fig.5|||||||||
31957|Jundelaya Hill Granodiorite|24197|6|Mentioned|p71 Tb. 7.1|||Of the Boolaloo Supersuite.||||||07-FEB-11
31957|Jundelaya Hill Granodiorite|50425|5|Briefly described|p1.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Province. Of the Boolaloo Supersuite.||||||07-NOV-08
31957|Jundelaya Hill Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite, monzogranite|
74834|Jungar Suite|64891|5|Briefly described|p34 Fig.2, p37 Fig. 2, p42, p52-53 Tb.1|Archean|Archean|Includes Illagalara and Chunderloo Monzogranites. Age: 2665Ma to ~2645ma. Geological province: Murchison Domain. Foliated to strongly sheared K-feldspar-porphyritic monzogranites.  Referred to as a Granite Suite in Fig. 2.||||||07-FEB-11
74834|Jungar Suite|65546|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Yilgarn Craton. 2665-2640 Ma. Consists of granites and metamorphic equivalents; high grade metamorphics, syenogranites and pegmatites; some parts deeply weathered..||||||
74834|Jungar Suite|65548|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Yilgarn Craton. 2665-2640 Ma. Includes Illigalara Monzogranite. Granites and metamorphic equivalents; high grade metamorphics, syenogranites and pegmatites; some parts deeply weathered. ||||||
74834|Jungar Suite|65550|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Includes Chunderloo Monzogranite as well as five other unnamed units, two of which show approximate ages of c. 2644 Ma and c. 2650 Ma. Suite age range shown as 2665 - 2640 Ma||||||
74834|Jungar Suite|66195|5|Briefly described|p605, p599 Fig.2|Neoarchean||In the Bald Rock Supersuite. Granites cut across Meeline Suite rocks and provide a minimum age constraint.|~2670 Ma.|||||13-MAR-12
74834|Jungar Suite|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Mapped as four separate units, only one of which - Chunderloo Monzogranite - is named.|||Includes Chunderloo Monzogranite and three un-named but separately mapped units.||Biotite metamonzogranite, commonly with abundant K-feldspar phenocrysts/porphyroclasts; muscovite metagranite, medium- to coarse-grained; metagranite interleaved with subordinate, foliated, metamorphic rock, gneissic banding locally developed.|
74834|Jungar Suite|67129|6|Mentioned|p18 Fig.19, p19 Fig.20, p57|Archean|Archean|Murchison Domain, Youanmi Terrane.|2665-2640 Ma||Chunderloo Monzogranite.||Metamonzogranites.|07-SEP-17
74834|Jungar Suite|68107|6|Mentioned|p618|||Western Youanmi Terrane.|||||Felsic magmatism in early stages.|
74834|Jungar Suite|68108|5|Briefly described|p628, p649|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. Appears as Supersuite in p649|ca. 2655-2640 Ma||||K-feldspar monzogranites.|
74834|Jungar Suite|68287|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Shown as older than D2 deformation (2665 - 2640 Ma).|2665 -2640 Ma||Informally subdivided in places into 5 unnamed units.||Biotite metagranite; dominantly metamonzogranite; minor metagranodiorite, metasyenogranite, metapegmatite; fine to coarse grained; locally gneissic.|
74834|Jungar Suite|68519|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|2665-2640 Ma||||Biotite metagranite; dominantly metamonzogranite; minor metagranodiorite, metasyenogranite, and metapegmatite; fine to coarse grained; locally gneissic.|
74834|Jungar Suite|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane.  Biotite monzogranite U-Pb zircon age: 2650 +/- 4 Ma as the magmatic crystallization age. Another biotite monzogranite of the Jungar Suite, sampled 22 km to the east, yielded a crystallization age of 2643 +/- 4 Ma (GSWA 187655, Wingate et al., 2012). From geochron file 187651.1.pdf.|2665-2640 Ma||Includes Illgalara Monzogranite, and 11 unnamed units, and Chunderloo Monzogranite?||Biotite metagranite; dominantly metamonzogranite; minor metagranodiorite, metasyenogranite, and metapegmatite; fine to coarse grained; locally gneissic|
74834|Jungar Suite|68698|5|Briefly described|p3-7, p10, p14-20, p27-28|Neoarchean|Neoarchean|Many plutons lie within high-strain, ductile strike-slip shear zones. Upper age is of crystallisation of a granite: Wingate et al. (2008). Geochemistry is discussed. REE plots. Lu-Hf isotope data and source regions discussed.|2665 +/- 5 Ma - 2640 Ma.||||Foliated to strongly sheared K-feldspar-porphyritic monzogranites.|
74834|Jungar Suite|69583|4|Described|p49, p51-53, p99, p103; Plate 2|Neoarchean|Neoarchean|Murchison Domain. Age range also given as 2655-2640 Ma.|2666-2640 Ma.||Chunderloo, Illgalara Monzogranites.|Is sheared against Windimurra Igneous Complex.|Mainly K-feldspar porphyritic biotite metamonzogranites.|
74834|Jungar Suite|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean||||Illgalara Monzogranite, Chunderloo Monzogranite|||
74834|Jungar Suite|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.|||Illgalara, Chunderloo Monzogranites.|||
74834|Jungar Suite|69626|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton|2665-2640 Ma||||Biotite metagranite; dominantly metamonzogranite; minor metagranodiorite, metasyenogranite, and metapegmatite; fine to coarse grained; locally gneissic.|
74834|Jungar Suite|69628|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|2665-2640 Ma||||Foliated meta biotite monzogranite; minor metagranodiorite, metasyenogranite, and pegmatite; fine- to coarse-grained; locally gneissic.|
74834|Jungar Suite|70020|5|Briefly described|p118|Neoarchean|Neoarchean|Geological province: Yilgarn Craton. HFSE-enriched granitic rocks.|||Includes Damperwah granite and Coolamen hornblende-biotite granite.|Overlain by Walganna Suite. Underlain by Tuckanarra Suite.||
74834|Jungar Suite|70030|5|Briefly described|p191-192|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton.|2655-2640 Ma||||K-Feldspar monzogranite.|17-JUL-19
74834|Jungar Suite|70139|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton.|||Chunderloo Monzogranite.|||
74834|Jungar Suite|70153|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean||2665 - 2640 Ma (inferred).||||Biotite metagranite; dominantly metamonzogranite; minor metagranodiorite, metasyenogranite, and metapegmatite; fine to coarse grained; locally gneissic.|
74834|Jungar Suite|70156|4|Described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma).|2657-2640 Ma (inferred)||||Biotite metagranite; dominantly metamonzogranite; minor metagranodiorite, metasyenogranite, and metapegmatite; fine to coarse grained; locally gneissic|
74834|Jungar Suite|70419|5|Briefly described|p12|||Density is 2.64-2.66 g/cm3.|||||Includes monzogranite and foliated metagranite.|
74834|Jungar Suite|70420|6|Mentioned|p9 Fig.6|Archean|Archean|||||||
74834|Jungar Suite|70794|4|Described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton. Also 2_5m_interpgeop15_lut.csv.|2665-2640 Ma inferred||||Biotite metagranite; dominantly metamonzogranite; minor metagranodiorite, metasyenogranite and metapegmatite; fine to coarse grained - locally gneissic.|
74834|Jungar Suite|70795|4|Described|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean||2665-2640 Ma||||Biotite metagranite; dominantly metamonzogranite, minor metagranodiorite, metasyenogranite and metapegmatite, fine to coarse grained.|
74834|Jungar Suite|70796|4|Described|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton granite. See also 100k_geologyl_lut.csv, 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 185929.1.pdf, 187651.1.pdf, 187655.1.pdf, Challa100_2541_stratig.pdf, Coolamaninu100_2540_stratig.pdf, Cue100_2443_stratig.pdf, Koonmarra100_2445_stratig.pdf, Madoonga100_2444_stratig.pdf, Nowthanna100_2643_stratig.pdf, Tieraco100_2545_stratig.pdf, Windimurra100_2641_stratig.pdf.|2665 to 2640 Ma (inferred)||Includes the Illgalara Monzogranite and the Chunderloo Monzgoranite.|Intruded by the Marlolmumbah Granite.|Biotite metagranite; dominantly metamonzogranite; minor metagranodiorite, metasyenogranite, and metapegmatite; fine to coarse grained; locally gneissic|
74834|Jungar Suite|70826|6|Mentioned|p9|Neoarchean|Neoarchean||||||Granites.|
74834|Jungar Suite|70830|5|Briefly described|p8-p10, p14|Neoarchean|Neoarchean|Murchison Domain. |c. 2655-2640 Ma||||K-feldspar monzogranite.|
74834|Jungar Suite|71168|5|Briefly described|p7|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Hosts HFSE-enriched intrusive rocks.|c. 2650 Ma||||Granitic rocks.|
74834|Jungar Suite|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma). Wingate et al. 2012 dated a biotite monzogranite at 2643+\-4 Ma. Sample GSWA 187651 (biotite monzogranite) yielded a weighted mean 207Pb/206Pb date of 2650+\-4 Ma, interpreted as the magmatic crystallization age of the biotite monzogranite. Sample GSWA 187655 (fine-graiend monzogranite) yielded a weighted mean 207Pb/206Pb date of 2643+\-4 Ma, interpreted as the magmatic crystallization age of the monzogranite. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|2665-2640 Ma||Includes Chunderloo Monzogranite, Illgalara Monzogranite.|Crosscut by Marlomumbah Granite.|Biotite metamonzogranite; metagranodiorite, metasyenogranite, and metapegmatite; fine to coarse grained; locally gneissic; metagranite interleaved with subordinate foliated metamorphosed mafic rock; granitic rock, foliated with minor metamafic rock|
74834|Jungar Suite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|2665-2640 Ma (inferred)||||Biotite metagranite; dominantly metamonzogranite; minor metagranodiorite, metasyenogranite, and metapegmatite; fine to coarse grained; locally gneissic|
74834|Jungar Suite|71271|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton.|||Chunderloo, Illgalara Monzogranites.||Metagranites, metamonzogranites, metamafic rocks, metagranodiorite, metasyenogranite, metapegmatite and granitic gneiss.|16-FEB-18
74834|Jungar Suite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||||Includes Chunderloo Monzogranite, Illgalara Monzogranite and 2 unnamed units.||Dominantly metamonzogranite; minor metagranodiorite, metasyenogranite, and metapegmatite; fine to coarse grained; locally gneissic; some foliated. Massive to foliated metagranitic rock interleaved with minor metamorphosed mafic rocks.|
74834|Jungar Suite|72389|5|Briefly described|Map Legend|Archean|Archean|Yilgarn Craton. Gabanintha 1:100k map sheet 2644. Includes several unnamed monzogranites.|||Includes the Chunderloo Monzogranite.|||28-AUG-20
74834|Jungar Suite|73410|6|Mentioned|p2|||Youanmi Terrane.|2665-2640 Ma.|||||
74834|Jungar Suite|73453|6|Mentioned|p2|||||||||
74834|Jungar Suite|73596|6|Mentioned|p1168|Neoarchean|Neoarchean|Yilgarn Craton.|2665-2640 Ma.|||||
33666|Jungle Monzogranite|24494|5|Briefly described|p38 App.1|||See also Jungle monzogranite.||||||
33666|Jungle Monzogranite|44203|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
33666|Jungle Monzogranite|60076|6|Mentioned|p45 App. 1|||[Agmju]   Biotite monzogranite.||||||
33666|Jungle Monzogranite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Biotite monzogranite.||||||07-FEB-11
33666|Jungle Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Biotite monzogranite.|06-AUG-15
33666|Jungle Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Biotite monzogranite.|
33666|Jungle Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
33666|Jungle Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. See 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|||||Biotite monzogranite|
77090|Jupiter Syenite|64633|5|Briefly described|p48, pp51-53.|||Forms a radial distribution of dykes into pillow basalt. Hosts the Jupiter gold deposit.|c.2665 Ma (inferred).|||||
31887|Juries Bore Granite|43854|5|Briefly described|Map Legend||Proterozoic|In the Lamboo Complex.||||||14-NOV-06
31887|Juries Bore Granite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31887|Juries Bore Granite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Paperbark Supersuite|||Cordierite-biotite-sillimanite syenogranite with abundant migmatitic metasedimentary inclusions; coarsely banded; fine to medium grained.|31-JUL-15
31887|Juries Bore Granite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Paperbark Supersuite|||Cordierite-biotite-sillimanite syenogranite with abundant migmatitic metasedimentary inclusions; coarsely banded; fine to medium grained.|
31887|Juries Bore Granite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone.|1861-1861 Ma (Inferred)|Unit of Paperbark Supersuite.|||Cordierite-biotite-sillimanite syenogranite with abundant migmatitic metasedimentary inclusions; coarsely banded; fine to medium grained|
31887|Juries Bore Granite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (183 -1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1861 Ma (inferred)|Unit of Paperbark Supersuite.|||Cordierite-biotite-sillimanite syenogranite with abundant migmatitic metasedimentary inclusions; coarsely banded; fine to medium grained|
76743|Kaarnka Group|68995|4|Described|p3-4, p7-10, p13-16, p20-22, p24 |Stenian|Stenian|Talbot Sub-basin. Age based on the Giles Event which occurred as this unit was deposited. Estimated to be approximately 3200m thick. The base of this Group may be a diamictite that overlies the Eliza Formation. Lithology discussed in great detail. Rhyolite from this Group is chemically separated into units A and B.  Geochemistry discussed. See also p27-29, p34, p43, p46, p49 Fig.25, p57, p61.|c. 1085-1040 Ma|Bentley Supergroup||Overlies the Mount Palgrave Group. Overlain by the Pussy Cat Group or the Cassidy Group.|Basal diamictite, massive to flow-banded feldspar or quartz-phyric rhyolite, intercalations of crystal-rich to -poor ignimbrite and lesser amounts of siliciclastic rocks. Minor basalt flows, quartz diorite and dolerite also occurs.|
76743|Kaarnka Group|69003|5|Briefly described|p51|Mesoproterozoic|Mesoproterozoic|Palgrave area, Talbot Sub-basin.|c.1070-c.1064 Ma.|||Is intruded by, or overlies, Winburn Granite.|Dominantly rhyolitic volcanic and pyroclastic rocks, with minor intercalations of basalt and sedimentary rocks.|
76743|Kaarnka Group|69009|5|Briefly described|Map Legend|Stenian|Stenian|Bentley Basin. Contains 10 unnamed units.|1068-1047 Ma||Includes the Kakalyalya Formation.||Mainly rhyolite as lava, tuffs and sills; lesser volcaniclastic conglomerate, sandstone and siltstone, basalt and basaltic andesite.|04-APR-14
76743|Kaarnka Group|69091|4|Described|p52 Fig.4.1, p54 Fig.4.2, see comments|||Talbot Sub-basin. Very unusual size (extent and volume) and facies association of volcanic rocks. Outcrops with very well developed and continuous flow-banding (in highly felsic rocks), including extensive evidence for rheomorphism, and high-temperature contact metamorphic assemblages in interflow sedimentary units. See also p59 Fig.4.6, p71 Fig.4.14, p75, p131 Fig.6.1.||Bentley Supergroup||Overlies Mount Palgrave Group; is overlain by Pussy Cat Group.|Dominantly ignimbritic rocks; subvolcanic rhyolite/dacite, rhyolite, basalt; magma compositions are water-poor but F-, alkali- and  FeO-rich, and reflect very high eruptive temperatures (>900 degrees C).|
76743|Kaarnka Group|69153|5|Briefly described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen||Bentley Supergroup|Kakalyalya Formation||Rhyolite as lavas, tuffs, and subvolcanic sills; trachytic to rhyolitic volcaniclastic siltstone and sandstone; rhyolite breccia, lapilli-tuff and tuff-breccia; volcanolithic pebble conglomerate; basalt and basaltic andesite|
76743|Kaarnka Group|69655|5|Briefly described|p3, p6, p66|Stenian|Stenian|Musgrave Region.|c. 1090-1040 Ma|Bentley Supergroup||||
76743|Kaarnka Group|69729|5|Briefly described|p66 Fig.1, p68, p70, p80, p82|||Talbot Sub-basin, Musgrave Province.||Bentley Supergroup.||Overlies the Mount Palgrave Group.|Dominated by feldspar(-quartz-)phyric rhyolite, and crystal-rich to crystal-poor ignimbrite, with lesser siliciclastic rocks and basalt flows.|
76743|Kaarnka Group|70095|5|Briefly described|p16-19|||Geological province: Musgrave Province. Of Talbot Sub-basin, Bentley Basin. Thickness of rhyolitic package: 2.8km; thickness of basaltic package: 0.2km. Generated over multiple eruptive events. See p19 Table 2 for U-Pb zircon data.||Unit of Pussy Cat Group.||Overlain by Kathleen Ignimbrite. Underlain by Mount Palgrave Group/Mount Waugh rhyolite.||
76743|Kaarnka Group|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|Musgrave Province/(Complex?) SHRIMP age from dacite sample (185415.1.pdf)|1047 Ma - 1077 Ma (Inferred) 1052 Ma (SHRIMP)|Bentley Supergroup|Includes Kakalyalya Formation||Basalt and basaltic andesite interbedded with volcaniclastic rhyolite, rhyolite, rhyolitic siltstone, ash tuff, rhyolitic sandstone and breccia, volcaniclastic breccia, conglomerate, diamictite; aphyric trachyte, pyroclastic siltstone and sandstone.|
76743|Kaarnka Group|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Sample GSWA 185415 (dacite) yielded an interpreted (regression intersecting concordia curve) igneous crystallisation age of 1052+\-5 Ma. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv.|1077-1047 Ma (inferred)|Unit of Bentley Supergroup.|Includes Kakalyalya Formation.||Aphyric trachyte, rhyolite; pyroclastic siltstone, autoclastic rhyolite breccia, basalt, basaltic andesite, rhyolite as porphyritic lava, tuff and subvolcanic sills, rhyolitic siltstone, trachytic to rhyolitic sandstone, volcanolithic conglomerate.|
76743|Kaarnka Group|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Bentley Basin.[mis]Spelt Karnka Group p5.||Bentley Supergroup||||20-APR-20
76743|Kaarnka Group|70831|5|Briefly described|p3, p5|||Musgrave Province.||Bentley Supergroup||||
76743|Kaarnka Group|71210|6|Mentioned|p5|||Talbot Sub-basin.||||||
76743|Kaarnka Group|71211|5|Briefly described|p6 fig 1.3, p7 fig 1.4, p24 fig 2.1|||Talbot Sub-basin. See also p25, p26, p27 fig 2.3, p84 fig 3.1, p86, p87 fig 3.2, p136 fig 4.1, p215-p216, p219, p234, p271.||Bentley Supergroup||Overlies the Mount Palgrave Group. Overlain by the Pussy Cat Group, apparently conformable.|Massive to flow-banded rhyolite with intercalated ignimbrites and lesser amounts of siliciclastic sedimentary rocks and basalts.|
76743|Kaarnka Group|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Succession of felsic volcanic rocks including extensive prolific pyroclastic units, some lava flows, and minor interbedded sedimentary rocks. Sample GSWA 185415 (dacite) yielded a regression intersecting concordia curve at 1052+\-5 Ma, interpreted as igenous crystallisation age of the dacite. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv.|1077-1047 Ma (inferred)|Unit of Bentley Supergroup.|Includes Kakalyalya Formation.||Aphyric trachite and rhyolite, authoclastic rhyolite breccia, basalt and basaltic andesite, rhyolite: feldspar-qtx porphyritic, flow banded, vitric and feldspar porphyritic; rhyolite laminated siltstone, sandstone, trachytic to rhyolitic sandstone.|
76743|Kaarnka Group|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1052+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Dacite.|
76743|Kaarnka Group|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Bentley Supergroup|||Rhyolitic and trachytic lavas, subvolcanic sills, and pyroclastic rocks, locally interlayered with volcanic sandstones and siltstones and minor basalt.|
76743|Kaarnka Group|72094|6|Mentioned|p3 Fig 2, p4|Mesoproterozoic|Mesoproterozoic|Talbot Sub-basin, Bentley Basin.||Unit of Bentley Supergroup.||||
76743|Kaarnka Group|72443|4|Described|p737-743, p747, p753|||Talbot Sub-basin. Has a combined stratigraphic thickness of around 3km. Mainly restricted to a NW-trending basin that forms the extent of the Kaarnka caldera structure which is the result of at least three independent caldera structures.|1045 +/- 8 Ma - 1021 +/- 24 Ma (SHRIMP U-Pb)|Bentley Supergroup||Overlies the Mount Palgrave Group.|Massive to flow-banded, feldspar-quartz phyric rhyolite, basalt and subvolcanic rhyolite/dacite.|
76743|Kaarnka Group|73437|6|Mentioned|p151|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Talbot Sub-basin.||Bentley Supergroup||||
35233|Kadgewarrina Monzogranite|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Of Carlindi Granitoid Complex.  Geological Province: Pilbara Craton.||||||07-NOV-08
35233|Kadgewarrina Monzogranite|24110|5|Briefly described|Plate 1|Archean|Archean|Belongs to Carlindi Granitoid Complex.  Geological Province: Pilbara Craton||||||07-NOV-08
35233|Kadgewarrina Monzogranite|24166|4|Described|p19|||Of the Carlindi Granitoid Complex||||||25-JUL-07
35233|Kadgewarrina Monzogranite|24193|5|Briefly described|p874, p875 Fig.2|Archean|Archean|Parent: Carlindi granitoid complex. Age: ca. 2890-2830 Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
35233|Kadgewarrina Monzogranite|24327|5|Briefly described|Map Legend|Archean|Archean|Of the Carlindi Granitoid Complex. Muscovite-biotite (-garnet) monzogranite. Age: c.2940Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
35233|Kadgewarrina Monzogranite|24349|5|Briefly described|Map legend|Archean|Archean|Of the Carlindi Granitoid Complex.  Age: c.2940Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
35233|Kadgewarrina Monzogranite|63420|5|Briefly described|Map legend|Archean|Archean|Of Split Rock Supersuite. Age: c.2860Ma. Geological Province: Pilbara Craton. Muscovite-biotite(-garnet) monzogranite; equigranular to weakly porphyritic; massive to layered.||||||07-NOV-08
35233|Kadgewarrina Monzogranite|63441|5|Briefly described|p12 tb. 2|Archean|Archean|Of Split Rock Supersuite. Age: c.2859Ma. Geological province: Pilbara Craton.||||||07-FEB-11
35233|Kadgewarrina Monzogranite|68281|5|Briefly described|Map Legend|Neoarchean|Mesoarchean|Pilbara Craton. The 4 facies are mapped separately. Minimum age from cross-cutting dykes.||Of the Split Rock Supersuite.||Includes enclaves of the Wilson Well Gneiss. Is intruded by dykes of Black Range Dolerite Suite.|Muscovite-biotite(-garnet) monzogranite, equigranular, massive to layered; biotite and biotite(-muscovite) monzogranites; garnet-tourmaline pegmatitic monzogranite with large, irregularly-shaped K-feldspar phenocrysts.|23-SEP-13
35233|Kadgewarrina Monzogranite|68283|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|c.2860 Ma (Wingate, 2003).|Of the Split Rock Supersuite.|||Muscovite-biotite(-garnet) monzogranite; equigranular to weakly porphyritic; massive to layered.|
35233|Kadgewarrina Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Muscovite--biotite(--garnet) monzogranite; equigranular to weakly porphyritic; massive to layered; fine to medium grained. Garnet-tourmaline pegmatitic monzogranite with large irregularly shaped K feldspar phenocrysts.|
35233|Kadgewarrina Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; Split Rock Supersuite Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|2851-2831 Ma (inferred)|Unit of Split Rock Supersuite.|||Muscovite-biotite(-garnet) monzogranite, biotite monzogranite, garnet-tourmaline pegmatitic monzogranite; numerous cross-cutting garnet-muscovite pegmatitic monzogranite dykes.|
35233|Kadgewarrina Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
35233|Kadgewarrina Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Muscovite-biotite(-garnet) monzogranite; equigranular to weakly porphyritic; massive to layered.|
76869|Kakalyalya Formation|69009|5|Briefly described|Map Legend|Stenian|Stenian|Bentley Basin.|1068-1047 Ma|Of the Kaarnka Group.|||Comprises quartz-feldspar-porphyritic rhyolite; subvolcanic intrusion; rounded and embayed quartz phenocrysts and subhedral and embayed alkali-feldspar phenocrysts, both up to 7 mm, in a very fine grained felsitic groundmass.|02-SEP-14
76869|Kakalyalya Formation|69153|5|Briefly described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen||Kaarnka Group|||Quartz-feldspar-porphyritic rhyolite; subvolcanic intrusion|
76869|Kakalyalya Formation|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic||1048 Ma - 1077 Ma (Inferred)|Kaarnka Group|||Quartz--feldspar-porphyritic rhyolite; subvolcanic intrusion; rounded and embayed quartz phenocrysts and subhedral and embayed alkali-feldspar phenocrysts, both up to 7 mm, in a very fine grained felsitic groundmass|
76869|Kakalyalya Formation|70793|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv.|1077-1047 Ma (inferred)|Unit of Kaarnka Group.|||Quartz-feldspar-porphyritic rhyolite; subvolcanic intrusion; rounded and embayed quartz phenocrysts and subhedral and embayed alkali-feldspar phenocrysts, both up to 7 mm, in a very fine grained felsitic groundmass|
76869|Kakalyalya Formation|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv.|1077-1047 Ma (inferred)|Unit of Kaarnka Group.|||Quartz--feldspar-porphyritic rhyolite; subvolcanic intrusion; rounded and embayed quartz phenocrysts and subhedral and embayed alkali-feldspar phenocrysts, both up to 7 mm, in a very fine grained felsitic groundmass|
26647|Kalgoorlie Group|22534|6|Mentioned|Fig.5 p10|||||||||
26647|Kalgoorlie Group|22666|5|Briefly described|p696|||||||||
26647|Kalgoorlie Group|22682|6|Mentioned|p12||Archean|Kambalda Supersequence||||||07-NOV-08
26647|Kalgoorlie Group|23137|4|Described|p245 Table.2|||||||||
26647|Kalgoorlie Group|23926|6|Mentioned|p16 Fig. 5|||||||||
26647|Kalgoorlie Group|24139|5|Briefly described|p239 Table 1|||Geological Province: Kambalda Domain.||||||
26647|Kalgoorlie Group|41368|6|Mentioned|Table 1|||||||||
26647|Kalgoorlie Group|41644|6|Mentioned|p219|||||||||
26647|Kalgoorlie Group|41670|6|Mentioned|p249|||||||||
26647|Kalgoorlie Group|41890|6|Mentioned|p278|||||||||
26647|Kalgoorlie Group|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
26647|Kalgoorlie Group|43052|5|Briefly described|Fig.3.8|||||||||
26647|Kalgoorlie Group|43162|6|Mentioned|5|||||||||
26647|Kalgoorlie Group|43496|6|Mentioned|6|||||||||
26647|Kalgoorlie Group|50548|5|Briefly described|p1174||Archean|Overlain by Black Flag Group.||||||07-FEB-11
26647|Kalgoorlie Group|60514|5|Briefly described|p25 Fig. 2, p36 Fig. 6, p65 Tb. 1|Archean|Archean|Includes; Paringa Basalt, Defiance Dolerite, Williamstown Dolerite, Kapai Slate, Devon Consols Basalt, Kambalda Komatiite, Lunnon Basalt. Age: 2690+/-5 - 2726+/-30 Ma.||||||09-OCT-12
26647|Kalgoorlie Group|60623|4|Described|p25 Fig.2|Archean|Archean|Geological Province: Eastern Goldfields.||||||07-NOV-08
26647|Kalgoorlie Group|60627|5|Briefly described|p65 Tb.1|||||||||
26647|Kalgoorlie Group|62108|5|Briefly described|p1409 Tb. 2|||Includes: Paringa Basalt, Williamstown Dolerite, Kapai Slate, Devon Consols Basalt, Hannan's Lake serpentinite, Kyarra Basalt, Pernatty Dolerite, Mutooroo Basalt, Kambalda Komatiite, Paringa Basalt, Defiance Dolerite, + Lunnon Basalt.||||||07-FEB-11
26647|Kalgoorlie Group|65204|6|Mentioned|pg6 Tbl.1|Archean|Archean|Komatiitic and tholeiitic basalt.||||||11-JUN-15
26647|Kalgoorlie Group|65834|5|Briefly described|p7, 45|||Kambalda Domain, Kalgoorlie Terrane. Hosts gold mineralisation in all parts of the succession.|||Paringa, Devon Consols, Lunnon Basalts; Defiance, Williamstown Dolerites; Kambalda Komatiite; Kapai Slate.||High Mg and tholeiitic basalt; massive, pillowed and vesicular lavas. Massive olivine adcumulate and/or thick komatiite flows, overlain by thin komatiite flows with minor interflow sedimentary beds; high Mg basalt at top.|
26647|Kalgoorlie Group|69583|5|Briefly described|p39|||Swager et al. (1995).|||Lunnon Basalt.|||
26647|Kalgoorlie Group|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2726 - 2680 Ma (age inferred).||Includes Bent Tree Basalt, Victorious Basalt, Two Sisters Subgroup, Hannans Subgroup.||Ultramafic schist, chert and banded chert, shale, sandstone, minor siltstone, basalt, plagioclase phyric basalt, basaltic breccia, komatiite, subordinate basalt; metamorphosed.|
26647|Kalgoorlie Group|70281|6|Mentioned|p454|||Norseman-Wiluna Fold Belt, Yilgarn Craton. Referred to as Kalgoorlie-Kambalda Group succession.|c.2730 to 2670 Ma.||||Predominantly greenstones: lower andesites and basalts, a regional marker unit of komatiites, upper basalts and rhyolites, and an uppermost sequence of flysch-type graywackes and molasse-type conglomerates.|
26647|Kalgoorlie Group|70290|6|Mentioned|p296|||Yilgarn Craton.|||Kambalda Komatiite.||Submarine volcanic rocks.|
26647|Kalgoorlie Group|71270|5|Briefly described|GEOL_LUT_CSV files|||Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|||Includes Broad Arrow Subgroup, Coolgardie Subgroup, Hannans Subgroup, Marshall pool Subgroup, Two Sisters Subgroup, Vetters Subgroup.||Basalt: variolitic, pyroxene spinifex-textured, plagioclase-phyric, metamorphosed; komatiite; peridotite, minor metapyroxenite: serpentinised, silicified; amphibolite, metabasalt, ultramafic schist, metamorphosed siliciclastics.|
26647|Kalgoorlie Group|72095|4|Described|p2,p3 Fig 2,4-6, 8-9|Neoarchean|Neoarchean|Eastern Goldfields, Yilgarn Craton. Comprises most of the lower mafic-ultramafic package in greenstone belts between Norseman and Leinster (Figs 1, 2). This group locally overlies, or is structurally juxtaposed against, poorly known, older (>2800 Ma) mafic-ultramafic successions.|2726-2680 Ma||Includes Two Sisters Subgroup, Marshall Pool Subgroup, Broad Arrow Subgroup, Vetters Subgroup, Coolgardie Subgroup and Hannans Subgroup.|||
26647|Kalgoorlie Group|72491|6|Mentioned|p5 Fig.4|||Kalgoorlie Terrane, Yilgarn Craton.||||||
26647|Kalgoorlie Group|73151|4|Described|p1-4, p6, p8, p10 Fig.6, p12-13, p15-16|Neoarchean|Neoarchean|Yilgarn Craton, Kalgoorlie Terrane. Basal part of stratigraphy in the Agnew Greenstone Belt. Locally up to 7 km thick. Well exposed around the Lawlers Anticline, divided into at least nine conformable units grouped into two magmatic cycles (Hayman et al., 2015). Also shown as including the White Hope Basalt, Satellite Igneous Complex, Bounty Igneous Complex, Turret Dolerite. Location in text includes p14 Fig.9.|ca. 2720 - 6290 Ma||Butchers Well Basalt, Donegal Komatiite, Hickies Bore Basalt, Fourteen Mile Well Formation, Songvang Formation, Never Can Tell Basalt, Agnew Komatiite, Burrell Well Basalt, Redeemer Basalt.|Equivalent to Agnew Greenstone Sequence, Unconformably underlies Mount White Group.|Dominated by mafic and ultramafic rocks including tholeiitic basalt, high-Mg basalt, gabbro, komatiite, differentiated gabbro-pyroxenite-peridotite sills, minor interflow units of thin, fine-grained sedimentary and silicic volcanogenic layers.|
26647|Kalgoorlie Group|73453|5|Briefly described|p3|Neoarchean|Neoarchean|Kalgoorlie Terrane.|2690-2660 Ma||||Intermediate to felsic volcanics.|
37153|Kaliranu Member|23414|5|Briefly described|Map Legend|Neoproterozoic|Mesoproterozoic|Of Lamil Group, Yeneena Basin||||||
37153|Kaliranu Member|23758|5|Briefly described|p10|Neoproterozoic|Neoproterozoic|Previously informally referred to as Kaliranu beds. Of Wilki Formation. Geological Province: Yeneena Basin. Max. thickness: >250 m.||||||
37153|Kaliranu Member|62453|4|Described|p69|Cryogenian|Cryogenian|Of the Wilki Formation. Shale, siltstone, sandstone, dolomite. Thickness: 200m+.||||||07-JAN-10
37153|Kaliranu Member|65454|5|Briefly described|p8|Cryogenian|Cryogenian|Siliciclastic. Upper part of  Wilki Formation.||||||
31780|Kalkan Supersuite|24197|5|Briefly described|p26, p100|Paleoproterozoic|Paleoproterozoic|Example of the Cullen Association. Age: 1780Ma. Geological Province: Paterson Province.||||||07-FEB-11
31780|Kalkan Supersuite|50436|5|Briefly described|p1.3, 2.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Paterson Orogen. Age: ~1780Ma. Intrudes the Rudall Complex.||||||07-NOV-08
31780|Kalkan Supersuite|63866|5|Briefly described|p141-p142, p148|||Talbot Terrane, Rudall Complex.|c. 1800 Ma-1760 Ma (Nelson, 1995)||||Felsic intrusive rocks.|
31780|Kalkan Supersuite|65454|5|Briefly described|p4-5|Statherian|Statherian|Smithies and Bagas (1997). Felsic intrusives. Cover approx 50% of Talbot Terrane by volume. Emplaced between about 1800-1760 Ma.||||||21-APR-16
31780|Kalkan Supersuite|67202|5|Briefly described|p184|||Part of the Rudall Complex; comprises 50% of the Talbot Terrane area. Corresponds with the Yambah Event.|1800-1760 Ma.||||Felsic intrusives.|
31780|Kalkan Supersuite|68981|5|Briefly described|p3-4, p13-19, p21-23, p25-27|||Budd et al. (2002). Intrudes eastern and western associations of the Talbot Terrane, and forms a major component of Connaughton Terrane, Rudall Province. Voluminous, high-K, metaluminous, calc-alkaline granites, with large K-feldspar phenocrysts and Sr-depleted, Y-undepleted trace-element patterns. U-Pb SIMS analyses and ages detailed. Origin of inherited zircons (specifically from Halfway Gneiss and Dalgaringa Supersuite) discussed in detail.|1801+/-12 Ma - 1762+/-13 Ma (Nelson, 1995).||||(Biotite)-monzogranite gneiss, granodiorite gneiss, muscovite quartzite, orthogneiss.|
31780|Kalkan Supersuite|69003|5|Briefly described|p4, p23, p40|Paleoproterozoic|Paleoproterozoic|Talbot and Connaughton Terranes, Paterson Orogen. A K-feldspar augen gneiss is dated at c.1777 Ma.|1800-1765 Ma.||||Voluminous felsic intrusive rocks.|
31780|Kalkan Supersuite|70084|5|Briefly described|p220,227|Statherian|Statherian|Geological province: Rudall Province, Paterson Orogen. Associated with Yapungku Orogeny. Characterised by a well-defined ND-mixing array that requires a juvenile ca. 1900 Ma component resembling Madura Province ans basement to Musgrave province (Kirkland et al., 2013b).||||||
31780|Kalkan Supersuite|71169|5|Briefly described|iv, p1, p3-p4, p6, p8, p11 fig 10|Orosirian|Orosirian|Dates provided are Sm/Nd; an additional age of 1781 +/- 4 Ma from a K-feldspar megacrystic biotite monzogranite (GA2005670162). See also p12-p13, p18, p21, p24, p31 fig 29, p51-p52, p54, p56-p60, p62-p67, p69-p70, p72, p87.|1804 +/- 3 Ma -1762 Ma (Kirkland et al., 2013a)||||Granitic gniess, monzogranite gneiss, layered granitic gneiss.|
31780|Kalkan Supersuite|71795|5|Briefly described|p31, p33-p34, p36, p38-p39, p41-p49|Statherian|Orosirian|Rudall Province. Interpreted to have been emplaced during the Yapungku Orogeny. Petrographic description and geochemsitry are briefly discussed, geodynamic implications are discussed in detail. Intrudes the Talbot and Connaughton terranes.|ca. 1804-1762 Ma||||Granitic gneisses including granodiorite gneiss and orthogneiss.|
31780|Kalkan Supersuite|73168|5|Briefly described|p739, p741 Fig.2, p742-743, p762-765|late Paleoproterozoic|mid Paleoproterozoic|Rudall Province, western. Talbot and Connaughton domains. Kalkan-aged igneous rocks are identified in the Tabletop Domain, considered an eastern extension of the Kalkan Supersuite based on age and overlapping zircon Hf-isotope compositions. Also suggests expanded age range of ca 1820-1750 Ma, may represent a number of distinct magmatic events. Yapungku Orogeny is proposed to incorporate the Kalkan Supersuite magmatism.|ca 1880-1750 Ma||||Includes sheet-like, felsic-intermediate augen orthogneiss. Granites. Deformed and metamorphosed.|
31780|Kalkan Supersuite|73214|5|Briefly described|p987|||Rudall Province.|1804-1762 Ma (Gardiner et al. 2018).|||||
75724|Kalkarindji Suite|68193|5|Briefly described|p44|||Kalkarindji Province. Heavily explored, geophysically anomalous locations have all proved negative for diamonds.|||||Basalts.|
75724|Kalkarindji Suite|69417|5|Briefly described|p2:6|Early Cambrian|Early Cambrian|Kalkarindji Province.|507 +/- 4 Ma.|||||12-JUL-16
75724|Kalkarindji Suite|69420|6|Mentioned|p5:81|Early Cambrian|Early Cambrian|Covered most of the North Australian Craton.||||||12-JUL-16
75724|Kalkarindji Suite|69422|6|Mentioned|p7:2 Fig.7.2|Cambrian|Cambrian|Kalkarindji Province.||||||12-JUL-16
75724|Kalkarindji Suite|69429|5|Briefly described|p14:4 Fig.14.7|Early Cambrian|Early Cambrian|Kalkarindji Province.|||||Includes basalt flows.|12-JUL-16
75724|Kalkarindji Suite|69432|5|Briefly described|p17:2, 4|Early Cambrian|Early Cambrian|Kalkarindji Province.||||Overlies Birrindudu Group.||12-JUL-16
75724|Kalkarindji Suite|69444|6|Mentioned|p29:5-6|||Shares geochemical similarities with the Indiana Suite in the southeastern Harts Range.|c.508 Ma.|||||12-JUL-16
75724|Kalkarindji Suite|69445|2|Defined|p30:1-12, 16-17|||Glass and Munson in Ahmad and Munson (2013). New name, after Kalkarindji township. Formerly Kalkarindji Volcanic Group of Kruse in Rawlings et al. (2008). Includes the igneous component of Kalkarindji Large Igneous Province, formerly the Kalkarinji (later revised by Glass and Phillip 2006) Continental Flood Basalt Province of Glass (2002). The definition excludes the minor intercalated sedimentary components of the former Group; they are included within the constituent Formations. 60-1100m thick; 760m thick at the type locality at Purnululu National Park, from WGS84 52K 426414mE 8078661mN to 428989mE 8079851mN. Four reference sections are detailed as are type sections for constituent Formations. Geochemistry and petrology described. Correlated with Mount Wright Volcanics and Cymbric Vale Formation (both Gnalta Group), Truro Volcanics, possibly Mooracoochie Volcanics.|||Antrim Plateau, Helen Springs, Colless, Table Hill Volcanics; Milliwindi Dolerite; Mount Ramsay dolerite.|Unconformably overlies Mount Forster Sandstone. Is overlain unconformably by Headleys, Montejinni, Tindall, Top Springs, Thorntonia Limestones; Tarrara, Gum Ridge, Wonarah Formations.|Tholeiitic basalt and dolerite with massive, porphyritic, partly vesicular (flow tops), amygdaloidal glomeroporphyritic textures, microdolerite, basaltic flow breccia, peperite, pyroclastic deposits.|12-JUL-16
75724|Kalkarindji Suite|69917|6|Mentioned|p175|||Geochemically similar to Coggans Gabbro.|ca 508 Ma|||||
75724|Kalkarindji Suite|70866|5|Briefly described|Map legend.|Cambrian|Cambrian|Kalkarindji Province.|||Includes Antrim Plateau Volcanics, Jindare Formation.|||01-MAR-18
75724|Kalkarindji Suite|70968|5|Briefly described|p6, p51, p100, p131, p137|Early Cambrian|Early Cambrian||||Helen Springs Volcanics.|Unconformably overlies Roper Group.|Basaltic volcanism.|
75724|Kalkarindji Suite|71267|6|Mentioned|1M_geologyp12_lut.csv|||||||||
75724|Kalkarindji Suite|71779|5|Briefly described|p5|Early Cambrian|Early Cambrian|||||Unconformably overlies the Roper Group.||24-SEP-18
75724|Kalkarindji Suite|71893|5|Briefly described|p41, p948|Cambrian|Cambrian|McArthur Basin.|507 +/- 4 Ma (Ar-Ar, Glass and Phillips 2006)|||Overlies the Jamison sandstone.||
75724|Kalkarindji Suite|73083|6|Mentioned|p: 1, 3, 12, 14-15, 17-18, 21, 24-25...|Cambrian|Cambrian|Strongly magnetic. Part of the Kalkarindji Continental Flood Basalt Province. Marked as Ebk on solid geology maps. Widespread in the Georgina Basin sequence. Associated with possible feeder dykes (labelled Ed - Cambrian dolerite) and altered Cambrian basalt is labelled Ebkl. [Written as Kalkarindji Igneous Suite on p30]. More locations p: 28-31, 34-35, 38, 42-45, 48-49, 55.||||Underlain by Kinevans Sandstone.|Basalt and agglomerate.|
79813|Kalli Formation|69583|5|Briefly described|p49|Mesoarchean|Mesoarchean|Murchison Domain.||Weld Range Group.||||
79813|Kalli Formation|69584|5|Briefly described|p5 Fig.2|Mesoarchean|Mesoarchean|||Weld Range Group||Overlain by the Madoonga Formation|Tholeiitic basalt.|
79813|Kalli Formation|69586|5|Briefly described|p22|Mesoarchean|Mesoarchean|Murchison Domain.||Weld Range Group.||||
32534|Kalmanyi Member|24371|5|Briefly described|p208|Famennian|Frasnian|Of the Napier Formation. Carbonate rich marginal slope strata. Geological province: Canning Basin.||||||
32534|Kalmanyi Member|64502|6|Mentioned|p785|||Of Napier Formation in Dingo Gap area.||||||10-NOV-08
32534|Kalmanyi Member|66127|5|Briefly described|p63, p245 Fig.326, p311, Plate 2.|Early Famennian|Late Frasnian|Named after a rock pinnacle which is a phallic symbol in an Aboriginal song cycle. Thickness is 230-240 m.||Unit in Napier Formation.|||Well-bedded to massive reefal-slope and fore-reef limestone; locally dolomitized, steeply dipping, with allochthonous blocks and debris flows in some horizons.|
28631|Kaluweerie Conglomerate|7471|5|Briefly described|Map Legend|Proterozoic|Proterozoic||||||Polymictic conglomerate and lithic sandstone.|
28631|Kaluweerie Conglomerate|23586|5|Briefly described|p17|||||||||
28631|Kaluweerie Conglomerate|23611|6|Mentioned|p21|Paleoproterozoic|Paleoproterozoic|See also page 33 Appendix 1. Geological Province: Yilgarn Craton.||||||07-NOV-08
28631|Kaluweerie Conglomerate|23759|6|Mentioned|p17|||||||||
28631|Kaluweerie Conglomerate|29378|3|Fully described|p129|||||||||
28631|Kaluweerie Conglomerate|35642|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Lower Proterozoic||||||07-NOV-08
28631|Kaluweerie Conglomerate|37460|5|Briefly described|p144|||||||||
28631|Kaluweerie Conglomerate|38978|6|Mentioned|p149|||||||||
28631|Kaluweerie Conglomerate|40938|6|Mentioned|p93|||||||||
28631|Kaluweerie Conglomerate|41635|5|Briefly described|p19|||||||||
28631|Kaluweerie Conglomerate|64580|4|Described|map legend||Proterozoic|Polymictic conglomerate and lithic sandstone.||||||15-DEC-08
28631|Kaluweerie Conglomerate|64586|5|Briefly described|Map legend|Proterozoic|Proterozoic|Polymictic conglomerate; arkose sandstone and mudstone.||||||
28631|Kaluweerie Conglomerate|65200|5|Briefly described|Map legend|Proterozoic|Proterozoic|Polymictic conglomerate and arkosic sandstone and mudstone, informally subdivided into two unnamed units. Of the Yilgarn Craton.|||informally subdivided into two unnamed units||Polymictic conglomerate and arkosic sandstone and mudstone,|24-NOV-09
28631|Kaluweerie Conglomerate|65264|5|Briefly described|p27, p44 Appdx. 1|Proterozoic|Proterozoic|On DEPOT SPRINGS. Comprises lower polymictic conglomerate with clasts including local granite, gneiss, basalt, BIF, and a matrix with little or no clay or silt; + upper lithic sandstone, fine- to coarse-gr., with clasts similar to those in conglomerate.||||||07-FEB-11
28631|Kaluweerie Conglomerate|69152|4|Described|GEOL_LUT_CSV files + geochron files|Proterozoic|Proterozoic|Metasandstone from this unit dated in 1998 U/Pb SHRIMP data. See geochron file 142860.1.pdf|Max deposit age: 2667+/-6 Ma||Informally subdivided into two units.||Polymictic conglomerate; arkosic sandstone and mudstone.|06-AUG-15
28631|Kaluweerie Conglomerate|69414|6|Mentioned|p88|Archean|Archean|Agnew-Wiluna Greenstone belt, Yilgarn Craton. Also presented as Kaluweerie Conglomeratic metasandstone.|2667 +/- 6 Ma (Nelson, 1998).||||Polymictic conglomerate and lithic sandstone.|
28631|Kaluweerie Conglomerate|69583|5|Briefly described|Plate 2|Proterozoic|Proterozoic||||||Polymictic conglomerate and lithic sandstone.|
28631|Kaluweerie Conglomerate|70153|5|Briefly described|100k_geologyp10_lut.csv|Proterozoic|Proterozoic|See also 500k_interpgeop14_lut.csv. 2667 Ma +/- 6 Ma (SHRIMP) age derived from sample of metasandstone (142860.1.pdf)|2500 - 541 Ma (inferred).||||Polymictic conglomerate, arkosic sandstone and mudstone.|
28631|Kaluweerie Conglomerate|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, mudstone|
28631|Kaluweerie Conglomerate|71270|4|Described|GEOL_LUT_CSV files|Proterozoic|Proterozoic|Geological province: West Australian Craton. Events: Western Australian Craton events (4000 - 570 Ma). See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv.|2500-541 Ma (inferred)||||Polymictic conglomerate and arkosic sandstone|
28631|Kaluweerie Conglomerate|72034|5|Briefly described|500k_interpgeop16_lut|Proterozoic|Proterozoic||||||Polymictic conglomerate and lithic sandstone.|
77093|Kambalda Sequence|63981|6|Mentioned|p91, p93 Fig.3, |Archean|Archean|One of four unconformity-bounded second-order sequences recognised in the Kalgoorlie Terrane. There is a formally-named unit, the Kambalda Supersequence.||||||
77093|Kambalda Sequence|64633|5|Briefly described|p4 Fig.3. |||Kalgoorlie Terrane.|c.2715 - c.2692 Ma.||Includes Paringa Basalt, Kapai Slate, D.C. Basalt, Kambalda Komatiite and Lunnon Basalt.|Is overlain by Kalgoorlie Sequence.||
77093|Kambalda Sequence|66880|4|Described|p7, pp25-26.|Archean|Archean|Redefined in this study. Apparently replaces the Kambalda Supersequence. The lowest of three lithostratigraphic divisions in the Kambalda Domain. Komatiitic and dacite-rhyolite volcanism 2707 - 2692 Ma.|c.2714 Ma (Hill et al. 1992) to c.2698 Ma.||Includes Lunnon Basalt, Kambalda Komatiite, Devon Consols Basalt and Paringa Basalt.|Is unconformably overlain by Black Flag Group.|Basalt and komatiite, with interlayered felsic rocks (dacite lavas and volcanogenic conglomerate).|
77093|Kambalda Sequence|67198|5|Briefly described|p5, p7, p48, p69-70, p81-84, p89, p112|Neoarchean|Neoarchean|See also p114, p118, p122, p136. Kalgoorlie Terrane. Hosts the komatiite-hosted Ni-sulfide mineralisation at Kambalda.|ca 2700 Ma||Lunnon Basalt, Kambalda Komatiite, Devon Consols Basalt, Kapai Slate, Paringa Basalt.|Is overlain unconformably by the Kalgoorlie Sequence. Is intruded by Kambalda Granodiorite.|Dominated by mafic-ultramafic rocks.|11-SEP-17
77093|Kambalda Sequence|68107|5|Briefly described|p617-619,  Fig.8, p621|Neoarchean|Neoarchean|Kalgoorlie Terrane. Age range given as c.2715-2692 Ma on p618.|ca. 2715-2704 Ma|||Underlain by the Penneshaw Formation ?|Mafic-ultramafic rocks.|
77093|Kambalda Sequence|68109|5|Briefly described|p660|Neoarchean|Neoarchean|Krapez et al. (2000). Older subdivision of the greenstone successions in the Kalgoorlie Terrane.|>2710 - c.2690 Ma|||Unconformably overlain by the Merougil and/or Kurrawang Sequence.|Tholeiitic and komatiitic mafic-ultramafics.|08-OCT-14
77093|Kambalda Sequence|68186|5|Briefly described|p4-5|Archean|Archean|Kalgoorlie Terrane, Eastern Goldfields Superterrane.|2715-2692 Ma.|||Is overlain by Kalgoorlie Sequence.|Mafic-ultramafic rocks.|
77093|Kambalda Sequence|68523|6|Mentioned|p122-123|||Mentioned in relation to Al-undepleted komatiites. This age is for assimilation-fraction crystallisation of volcanic suites in the Sequence.|~2.7 Ga.|||||
77093|Kambalda Sequence|69091|5|Briefly described|p31, p32|||Of Kalgoorlie Terrane in western part of Eastern Goldfields Superterrane.|c. 2715-2692 Ma e.g. Kositcin et al. (2008)||||Basalt.|
77093|Kambalda Sequence|69404|6|Mentioned|p4, p4 Fig.4|Neoarchean|Neoarchean|Kalgoorlie Terrane. Attributed to a major plume event. |2710-2690 Ma|||Overlain by the Kalgoorlie Sequence.|Tholeiitic to komatiitic mafic rocks.|
77093|Kambalda Sequence|69586|5|Briefly described|p1-2|||Western Kalgoorlie Terrane.|2715-2692 Ma.|||Is overlain by the Kalgoorlie Sequence.|Mafic-ultramafic rocks.|
77093|Kambalda Sequence|69631|6|Mentioned|p26||||||Includes Lunnon Basalt.|||
77093|Kambalda Sequence|70020|4|Described|p117,121|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton. Mafic-ultramafic succession in the Kalgoorlie Terrane, related to a major plume event in the Yilgarn Craton at 2.72 Ga, broadly contemporaneous with komatiitic magmatism in the Wattagee Formation and emplacement of the Yalgowra Suite.|2710-2692 Ma||Includes Paringa Basalt, Kapai Slate, D. C. Basalt, Kambalda Komatiite and Lunnon Basalt.|Overlain by Spargoville Formation/Kalgoorlie Sequence.||
77093|Kambalda Sequence|70276|6|Mentioned|p783|||Kalgoorlie terrane, Yilgarn Craton.Time-equivalent to the Agnew-Wiluna greenstone belt.|||||Mafic-ultramafic sequence.|
77093|Kambalda Sequence|70326|5|Briefly described|p337|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton. Comprises ?2715-2690 Ma komatiite and basalt intercalatedwith interflow sediments, and ?2710-2690 TTG dacitic volcanicand volcaniclastic rocks (Barley et al., 2008; Kositcin et al., 2008).|~2715-2690 Ma|||Overlain conformably by Kalgoorlie Sequence.||
77093|Kambalda Sequence|70482|5|Briefly described|p317-318, 320, 323|Archean|Archean|Envelops the Scotia-Kanowna Dome batholith, Eastern Goldfields Superterrane, Eastern Yilgarn Craton. Un-named units include a volcaniclastic unit, a lower basalt (~2720 Ma), dacite (2707 Ma), komatiite (~2707 Ma), and an upper basalt (2687 Ma): all described. Deformations described.|||Spargoville Formation.|Is overlain by the Kalgoorlie Sequence.|Greenstone stratigraphy: lavas, high-level intrusions and volcaniclastic units.|
77093|Kambalda Sequence|70773|5|Briefly described|p18 fig 11|||Kambalda Domain, Kalgoorlie Terrane.|||Includes the Lunnon Basalt, Kambalda Komatiite, Devon Consols Basalt and the Paringa Basalt.|||
77093|Kambalda Sequence|71148|5|Briefly described|p121-122, 131, 135, 138-139|Neoarchean|Neoarchean|Kalgoorlie Terrane, Eastern Goldfields Superterrane, Yilgarn Craton. At least two cycles of plume-related magmatism recognised. Hosts the Nimbus base metal deposit.|2720-2690 Ma.||Includes Lunnon, Devon Consols, Paringa Basalts.|Is overlain by Kalgoorlie Sequence.|Mafic-ultramafic.|
77093|Kambalda Sequence|71168|5|Briefly described|p8-p9|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton.|c. 2710-2692 Ma|||Overlain by the Kalgoorlie Sequence.|Mafic-ultramafic rocks.|
77093|Kambalda Sequence|71308|6|Mentioned|p711 Fig.2|||Kalgoorlie Terrane.||||||
77093|Kambalda Sequence|71309|6|Mentioned|p740||||||||Includes mafic to ultramafic flows.|
77093|Kambalda Sequence|72049|4|Described|p253, p255-p256, p258-p262, p268|Neoarchean|Neoarchean|SHIRMP aand LAICPMS analytical techniques and results are discussed in detail. Roughly 2710-2690 Ma. Also includes the Paringa Basalt, Defiance Dolerite, Hannans Lake Serpentinite, Spargoville Formation, Agnew Ultramafic, Lawlers Basalt.|2692 +/- 4 Ma (Claoue-Long et al., 1988)||Includes the Noganyer Formation, Woolyeenyer Formation, Lunnon Basalt, Kambalda Komatiite, Devon Consols Basalt, Kapai Slate.|Overlain by the Kalgoorlie Sequence. Intruded by the Powder Sill Gabbro.|Massive frame-work supported feldspar-rich granule breccia intercalated with black mudstone.|
77093|Kambalda Sequence|72057|5|Briefly described|p237-238, 242|Neoarchean|Neoarchean|Geological province: Yilgarn Craton. Thick pile of mafic and ultramafic units with thin interflow sedimentary units (Krapez et al., 2008).|c. 2720-2690 Ma|||Overlain conformably to unconformably by Kalgoorlie Sequence/Black Flag Group.||10-JAN-23
77093|Kambalda Sequence|72485|5|Briefly described|p2-3,|||The lower portion of the Kalgoorlie Terrane stratigraphy. Hosts the high-grade Nimbus deposit, which this study argues is a syn-volcanic, replacement-type VHMS deposit dated at c.2703 Ma.|2720-2690 Ma.||Paringa, D.C., Lunnon Basalts; Kambalda Komatiite; Kapai Slate.|Is overlain by the Kalgoorlie Sequence.|Includes plume-related, mafic-ultramafic rocks. The original stratigraphy included glassy quartz-plagioclase phyric dacite (replaced by massive sulphide mineralisation hosting Ag-Zn(-Au) deposits), carbonaceous mudstones, polymict conglomerates.|
77093|Kambalda Sequence|72491|6|Mentioned|p40|||Large volumes of granite are interpreted to have pooled immediately below this unit, producing a regional-contact type of metamorphism at 2685-2665 Ma.||||||
77093|Kambalda Sequence|73238|5|Briefly described|p18|||Kambalda district, Eastern Goldfields Terrane. Thought to be associated with early rifting.|2715-2690 Ma.|||Is overlain by the Black Flag Group.|A greenstone sequence, predominantly komatiite and basalt intercalated with sedimentary rocks and c.2710-2690 Ma dacitic volcanic and volcaniclastic rocks.|
77093|Kambalda Sequence|73300|6|Mentioned|p1112-1113|||Yilgarn Craton, Kalgoorlie terrane.|||Hannan's Lake Serpentinite, Devon Consols Basalt, Kapai Slate, Paringa Basalt.|Underlies the Kalgoorlie Sequence.||
77093|Kambalda Sequence|73391|6|Mentioned|Appendices.|||Gresham and Loftus-Hills (1971). Regional stratigraphic correlation chart of other workers.|||||In ascending order: Kambalda hangingwall basalt lower member, sediment-intrusive complex, Kambalda hanging-wall basalt upper member.|
34368|Kambalda Supersequence|22682|5|Briefly described|p12||Archean|Yilgarn Craton||||||07-NOV-08
23680|Kamilili Formation|13194|4|Described|p392 Tb. 4-16, p402 fig 4-66|Famennian|Famennian|Type Section: near Tanmurra Bore 15o06'S 128o38'E. 160-750m thick basinal to marginal slope facies.||Ningbing Group||Overlies Djilirri Limestone (unconformably). Laterally equivalent to Garimala Limestone, Wungabal Limestone, Djilirri Limestone.|Fossiliferous limestone, shale and limestone breccia.|
23680|Kamilili Formation|40993|2|Defined|p8|Famennian|Famennian|||||||
23680|Kamilili Formation|41864|3|Fully described|p89|||||||||
23680|Kamilili Formation|41865|5|Briefly described|Map legend|late Famennian|early Famennian|||||||
23680|Kamilili Formation|41867|5|Briefly described|Map legend|late Famennian|early Famennian|||||||
23680|Kamilili Formation|42030|5|Briefly described|p749|||||||||
23680|Kamilili Formation|42933|5|Briefly described|Fig.94 p258|||||||||
23680|Kamilili Formation|64580|6|Mentioned|map legend|||Of Ningbing Group.||||||15-DEC-08
23680|Kamilili Formation|69099|5|Briefly described|500k_geologyp08_lut.csv|Late Devonian|Late Devonian|||Ningbing Group||||
23680|Kamilili Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Famennian|Frasnian|||||||
23680|Kamilili Formation|69452|6|Mentioned|p36:7|||||Ningbing Group.||||12-JUL-16
23680|Kamilili Formation|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Ningbing Group.||||
23680|Kamilili Formation|69673|6|Mentioned|p169|||||Ningbing Group||Overlain by Wungabal Limestone, overlies Djilirri Limestone||
32223|Kangaroo Caves Formation|22441|5|Briefly described|p14|||Pilbara Craton. Overlies Strelley Granite. Overlain by Gorge Creek Group.||||||17-SEP-08
32223|Kangaroo Caves Formation|23389|5|Briefly described|p10|||||||||
32223|Kangaroo Caves Formation|23416|5|Briefly described|Map Legend|Archean|Archean|Of Sulphur Springs Group, Pilbara Craton||||||07-NOV-08
32223|Kangaroo Caves Formation|23755|4|Described|p37|Archean|Archean|See also page 17 table 1. Age: 3238-3235 Ma. Of Sulphur Springs Group. Max. thickness: 1500 m.||||||07-NOV-08
32223|Kangaroo Caves Formation|23783|5|Briefly described|p16|Archean|Archean|Of Sulphur Springs Group.||||||07-NOV-08
32223|Kangaroo Caves Formation|23784|5|Briefly described|p59|Archean|Archean|||||||07-NOV-08
32223|Kangaroo Caves Formation|23891|5|Briefly described|p91|Archean|Archean|Of Sulphur Springs Group. Geological Province: Pilbara Craton. See also page 95.||||||07-NOV-08
32223|Kangaroo Caves Formation|23956|4|Described|p1264|Archean|Archean|Age: ca. 3.24 Ga. Overlies the Strelley Granite. Of the Sulphur Springs Group. Geological Province: Pilbara Craton.||||||07-NOV-08
32223|Kangaroo Caves Formation|24025|4|Described|p8 Tb. 1|Archean|Archean|Of Sulphur Springs Group. Differentiated volcanic-volcaniclastic pile of a mainly tholeiitic sequence of basalt to rhyolite, with comagmatic granitoid. Max. thickness: ~1700 m. Geological Province: Pilbara Craton.||||||15-APR-13
32223|Kangaroo Caves Formation|24184|5|Briefly described|p702, p699 Fig.5|Archean|Archean|Parent: Sulphur Springs Group. Underlying Unit: Kunagunarrina Formation. Geological Province: Pilbara Craton. Max Thickness: 1.5 km. Age: ca. 3507-3467 Ma||||||15-APR-13
32223|Kangaroo Caves Formation|24185|5|Briefly described|p734|Archean|Archean|Age: ca. 3240 Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
32223|Kangaroo Caves Formation|24531|4|Described|p20, p5 Tb. 1|Archean|Archean|Of the Sulphur Springs Group. Age: c.3238-3235 Ma. Conformably overlies the Kunagunarinna Formation. Max. thickness: 200 m. Geological Province: Pilbara Craton.||||||15-APR-13
32223|Kangaroo Caves Formation|24532|5|Briefly described|Map legend|Archean|Archean|Of the Sulphur Springs Group (Pilbara Supergroup).  Age: c.3240Ma.||||||07-NOV-08
32223|Kangaroo Caves Formation|24550|5|Briefly described|p31 Tb. 3.1|Archean|Archean|Of the Sulphur Springs Group. Tholeiitic mafic to felsic volcanics, chert, BIF. Age: 3238-3235 Ma. Max. thickness: 1.5 km. Geological Province: Pilbara Craton.||||||15-APR-13
32223|Kangaroo Caves Formation|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Of Sulphur Springs Group. Differentiated volcanic-volcaniclastic pile of mainly tholeiitic magmatic affinity varying from basalt to rhyolite. Age: 3238- 3235 Ma.||||||15-APR-13
32223|Kangaroo Caves Formation|50379|5|Briefly described|Map Legend|Archean|Archean|Of Sulphur Springs Group (Pilbara Supergroup). Geological Province: Pilbara Craton.||||||07-NOV-08
32223|Kangaroo Caves Formation|50544|5|Briefly described|p40|Archean|Archean|Of the Sulphur Springs Group.||||||07-NOV-08
32223|Kangaroo Caves Formation|61205|5|Briefly described|p548, p548 Fig. 1|||Geological Province: Pilbara Craton. Of the Sulphur Springs Group. Underlain by Strelley Granite. Tholeiitic volcanic strata.||||||31-MAY-07
32223|Kangaroo Caves Formation|61253|5|Briefly described|p51|Archean|Archean|Of the Sulphur Springs Group. Geological Province: Pilbara Craton.||||||15-APR-13
32223|Kangaroo Caves Formation|61256|5|Briefly described|p340 Fig. 5b|Archean|Archean|Of the Sulphur Springs Group.||||||07-NOV-08
32223|Kangaroo Caves Formation|61266|5|Briefly described|p58 Tb.1, p59|Archean|Archean|Of the Sulphur Springs Group. Age: 3238-3235 Ma (R. Buick, 1997, pers. comm.). Overlies Kunagunarrina and Leilira Fms. Max. thickness: ~1700m. Differentiated volcanic-volcaniclastic pile. Geol. Prov: Pilbara Craton||||||07-NOV-08
32223|Kangaroo Caves Formation|61579|5|Briefly described|p58 Fig. 2|Archean|Archean|Of the Sulphur Springs Group. Age: 3238-3235Ma. ||||||07-NOV-08
32223|Kangaroo Caves Formation|63110|6|Mentioned|p1125 Fig. 5|||Comprised felsic volcanics, andesite-basalt and microdiorite.||||||
32223|Kangaroo Caves Formation|63420|5|Briefly described|Map legend|Archean|Archean|Of Sulphur Springs Group (Pilbara Supergroup). Geological Province: Pilbara Craton. Felsic volcanic and siliciclastic sedimentary rocks; metamorphosed.||||||15-APR-13
32223|Kangaroo Caves Formation|63441|5|Briefly described|p4 Tb. 1|Archean|Archean|Of Sulphur Springs Group (Pilbara Supergroup).||||||15-APR-13
32223|Kangaroo Caves Formation|63538|4|Described|p15, p16, p6 Fig. 3|Archean|Archean|Of Sulphur Springs Group. Overlain by Budjan Creek Formation, underlain by Kunagunarrina Formation. Geological Province: Pilbara Craton. Rhyolitic volcanic rocks.||||||19-APR-13
32223|Kangaroo Caves Formation|63649|5|Briefly described|p201 Fig. 2|Archean|Archean|Of Sulphur Springs Formation (Pilbara Supergroup). Age: 3.240 Ga. Geological Province: Pilbara Craton.||||||15-APR-13
32223|Kangaroo Caves Formation|64328|5|Briefly described|p56 Tb. 1|||Of Sulphur Springs Group. Felsic volcanic rocks, andesite, chert.||||||07-FEB-11
32223|Kangaroo Caves Formation|64405|5|Briefly described|p4 Fig. 3|Archean|Archean|Name inferred from Kangaroo Caves only in Figure 3. Of the Sulphur Springs Group (De Grey Supergroup). Felsic rocks.||||||07-FEB-11
32223|Kangaroo Caves Formation|65757|5|Briefly described|p83 Fig. 3|Paleoarchaen|Paleoarchaen|Includes dacite, underlies the Marker Chert. Age: 3235+/-3 Ma.||||||
32223|Kangaroo Caves Formation|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Sulphur Springs Group. Includes Pincunah Banded-iron Member. Aged 3252-3235 Ma. Felsic and mafic volcanic rocks, and siliciclastic sedimentary rocks; metamorphosed.||||||
32223|Kangaroo Caves Formation|66745|4|Described|p53 Fig.3, p54 Fig.4.|Paleoarchean|Paleoarchean|Hydrothermal activity, with deep-water chemical sedimentation and VMS mineralization.|3252-3235 Ma.|Unit in Sulphur Springs Group.|Includes Pincunah Banded-iron Member.|Overlies Kunagunarinna Formation.|Felsic volcanic rocks, chert, banded iron-formation.|
32223|Kangaroo Caves Formation|67130|5|Briefly described|p16, p20 fig 13|Paleoarchean|Paleoarchean|Up to 1500m thick. Felsic rocks of this formation thin laterally away from the thickest part of this group into banded iron formation (the Pincunah Member)|3245 Ma - 3235 Ma|Sulphur Springs Group|Includes Pincunah Member|Overlies Kunagunarrina Formation|Andesite-to basalt-rhyolite volcanic rocks, capped by silicified epiclastic and siliciclastic rocks.|
32223|Kangaroo Caves Formation|67197|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.|3251-3235 Ma.|Sulphur Springs Group.||||
32223|Kangaroo Caves Formation|67201|5|Briefly described|p7 Fig.4, p12 Tb.1|||In northern Pilbara Craton, East Pilbara Terrane.|c. 3235 Ma|Sulphur Springs Group||||
32223|Kangaroo Caves Formation|67269|5|Briefly described|p6 Fig.3|Paleoarchean|Paleoarchean|||Sulphur Springs Group.|Pincunah Banded-iron Member.|Overlies Kunagunarinna Formation.|Felsic volcanic rocks; chert, BIF.|
32223|Kangaroo Caves Formation|67270|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Sulphur Springs Group.|Pincunah Banded-iron Member.|||
32223|Kangaroo Caves Formation|67668|5|Briefly described|Fig. 2-4; p.156-157; Tb.1. ||Paleoarchean|East Pilbara Terrane, Pilbara Craton. Containing one of Earth's oldest and best-preserved VHMS deposits. Possible evidence of early life is reviewed. |ca. 3240 Ma.|Sulphur Springs Group||Overlies the Kunagunarrina Formation, underlies the Cardinal Formation (Soanesville Group)|Volcanic hosted massive sulfide deposiit, overlain by silicified sediments.|17-SEP-14
32223|Kangaroo Caves Formation|68035|4|Described|p293, p288 Fig 4|Paleoarchean|Paleoarchean|Pilbara Supergroup, East Pilbara Terrane, Pilbara Craton. Includes stromatolites, microbial mats or microfossils deposited around hot springs or hydrothermal vents.|3252 - 3235 Ma|Of Sulphur Springs Group.|Includes Pincunah Banded-iron Member.|Overlies Kunagunarinna Formation.|Felsic volcanics, chert, BIF|
32223|Kangaroo Caves Formation|68280|5|Briefly described|p4||||3252-3235 Ma|Sulphur Springs Group|Includes Pincunah Banded-iron Member|Overlies Kunagunarinna Formation|Felsic volcanic rocks.|
32223|Kangaroo Caves Formation|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|3252-3235 Ma (Buick et al. 2002).|Of the Sulphur Springs Group.|||Metamorphosed polymictic cobble conglomerate with clasts of altered komatiitic basalt; metamorphosed felsic volcanic sandstone (tuffaceous) with local chert and quartz-sericite schist.|
32223|Kangaroo Caves Formation|68282|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|3252-3235 Ma (Buick et al. 2002).|Of the Sulphur Springs Group|Includes Pincunah Banded Iron Member.||Banded iron-formation, jaspilitic, minor layered chert and shale; white, grey and black layered chert, includes felsic volcaniclastic sandstone and shale; andesite and minor basalt, pillowed or massive, local dolerite sills; all metamorphosed.|
32223|Kangaroo Caves Formation|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c. 3240-3235 Ma (Buick et al. 2002).|Of the Sulphur Springs Group.|||Felsic volcanic and siliciclastic sedimentary rocks; metamorphosed.|
32223|Kangaroo Caves Formation|68284|5|Briefly described|p7|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Microfossils have been reported from upper part of this unit.||Sulphur Springs Group.|Pincunah Banded-iron Member.|Overlies Kunagunarinna Formation.||
32223|Kangaroo Caves Formation|69013|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|Includes 4 unnamed facies. Age from andesitic volcanic sandstone at the base of this unit.|c.3242 Ma|Of the Sulphur Springs Group.|Includes the Pincunah Banded-Iron Member.||Jaspilitic banded iron-formation, layered chert and shale; metarhyolite; layered chert, felsic volcaniclastic sandstone and shale; andesite and minor basalt, local dolerite sills; andesitic volcanic sandstone; all metamorphosed.|30-APR-14
32223|Kangaroo Caves Formation|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Mapped as 9 separate unnamed sub-units. See map legend for a detailed lithological description.|3252-3235 Ma (Buick et al. 2002)|Of the Sulphur Springs Group.|Includes the Pincunah Banded-Iron Member.||Olistostrome megabreccia; banded iron-formation; layered chert; shale; andesite; andesitic volcanic sandstone; dacite and rhyodacite; felsic volcanic rocks; felsic volcanic breccia and volcaniclastic sandstone; rhyolite lava and pumice breccia.|02-MAY-14
32223|Kangaroo Caves Formation|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Metarhyolite, schistose metafelsic volcanic rocks; quartz sericite schist. Age derived from sample of metamorphosed rhyolite and rhyolitic volcaniciclastic rock (160956.1.pdf, 160957.1.pdf) and constrains crystallisation of the protoliths.|3245 Ma +/- 2 Ma -3192 +/- 21 Ma (SHRIMP)|Sulphur Springs Group|Includes Pincunah Banded-Iron Member,||Olistostrome megabreccia, shale; metamorphosed.  Polymictic cobble conglomerate, layered chert. Andesite and andesitic volcanic sandstone, dacite and rhyodacite. Rhyolite lava, felsic and mafic volcanic rocks, volcanic and pumice breccia .|
32223|Kangaroo Caves Formation|69301|4|Described|p5 Fig.3, p9 Tb.1, p20 Tb.2|||Pilbara Craton. East Pilbara Terrane. Pilbara Supergroup successions include thick felsic volcanic formations, each contemporaneous with the four granitic supersuites. i.e. Kangaroo Caves and Cleland Supersuite.|3252-3235 Ma|Sulphur Springs Group|Pincunah Banded-iron Member||Felsic volcanic rocks.|
32223|Kangaroo Caves Formation|69548|6|Mentioned|p2|||Soanesville greenstone belt, East Pilbara terrane. Hosts massive sulphide mineralisation, and hydrothermal mineralisation analogous to modern-day black smokers, driven by heat from the intrusion.||Topmost Sulphur Springs Group.|||Felsic volcanics and a marker chert.|
32223|Kangaroo Caves Formation|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Formerly mapped as part of the Golden Cockatoo Formation (Van Kranendonk and Morant, 1998; Van Kranendonk, 2000). Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA 160956 (metarhyolite) yielded an interpreted magmatic crystallisation age of 3245+\-2 Ma (207Pb/206Pb concordia age). Sample GSWA 160957 (felsic volcaniclastic rock) yielded an interpreted maximum depositional age of 3242+\-21 Ma for the sedimentary protolith (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.|3255-3235 Ma (inferred)|Unit of Sulphur Springs Group.||Intruded by Dalton Suite. Underlain by Euro Basalt or Soanesville Group.|Andesite, andesitic volcanic sandstone, basalt, dacite and rhyodacite, felsic volcanic and volcaniclastics, metarhyolite, chert, olistostrome breccia.|
32223|Kangaroo Caves Formation|69616|4|Described|p159-164, p171-177, p179-182, p184|Archean|Archean|Cut by NE-striking sub-vertical faults which commonly converge at depth, but do not extend far into overlying Soanesville Group. Mineralisation discussed.|c.3240 Ma.|Unit in Sulphur Springs Group.|Includes Marker Chert.|Overlies Kunagunarrina Formation. Is overlain by Soanesville Group. Is intruded by Strelley Granite.|Predominantly tholeiitic volcanic rocks: andesite-basalt, rhyolite, dacite, rhyodacite dome; overlain by a regionally extensive layer of chert.|
32223|Kangaroo Caves Formation|70022|6|Mentioned|p115|||East Pilbara Terrane.||Sulphur Springs Group.||||
32223|Kangaroo Caves Formation|70775|6|Mentioned|p12, p24 |||East Pilbara.||Sulphur Springs Group||Overlies the Kunagunarinna Formation.||
32223|Kangaroo Caves Formation|70884|5|Briefly described|p123|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|3.25-3.24 Ga|Unit of Sulphur Springs Group.||Overlain by . Underlain by Kunagunarinna Formation.||
32223|Kangaroo Caves Formation|71041|5|Briefly described|p43, p45 fig 2|Paleoarchean|Paleoarchean|East Pilbara Terrane. |~3230 Ma|Sulphur Springs Group|Includes the Pincunah banded iron member.|Intruded by the Dalton Suite.||10-NOV-17
32223|Kangaroo Caves Formation|71137|6|Mentioned|p4|Archean|Archean|Pilbara.|3240 +/- 2 Ma (U-Pb TIMS; van Kranendonk, 2000).|Sulfur Springs Group.|||Includes a dacite tuff.|
32223|Kangaroo Caves Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Sulphur Springs Large Igneous Province, East Pilbara Terrane.|Max age 3253+/-4 Ma, min 3235+/-3 Ma.|Sulphur Springs Group|||Felsic and mafic volcanic rocks, and siliciclastic sedimentary rocks; metamorphosed.|
32223|Kangaroo Caves Formation|72064|5|Briefly described|p66|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Sulphur Springs Group.||Underlain by Kunagunarinna Formation.||
32223|Kangaroo Caves Formation|72668|5|Briefly described|p4-6, p8, p24|||East Pilbara Terrane. Up to 1500m thick.|c. 3240 Ma|Sulphur Springs Group|Includes the Pincunah Member.|Overlies the Kunagunarinna Formation.|Andesite and basalt through to rhyolite capped by silicified epiclastic and siliciclastic rocks.|13-JAN-22
23682|Kangiangi Clay|38776|3|Fully described|p40|||||||||
23682|Kangiangi Clay|40987|6|Mentioned|p34|||||||||
23682|Kangiangi Clay|61155|5|Briefly described|p16|Middle Miocene|Early Miocene|Overlies and interfingers with Millstream Dolomite; overlain by Weelumurra beds. Thickness: 46m. Geological Province: West Fortescue Valley. ||||||
23682|Kangiangi Clay|63372|5|Briefly described|Map Legend|Pleistocene|Miocene|Alluvial silt and Clay, indurated.||||||
23682|Kangiangi Clay|65194|5|Briefly described|p15-16 Figs.2.3,2.4, p.100-102, p.108|Pleistocene|Late Neogene|Late Neogene lacustrine deposit: indurated silty and clayey alluvium; calcareous in upper part, basal pisolite gravel. Unconformably overlies the Robe Formation and the Millstream Dolomite. Max thicknexx 47 m.||||||06-APR-16
35672|Kanowna Belle Porphyry|23142|5|Briefly described|p203 Fig.2|||||||||
35672|Kanowna Belle Porphyry|23796|5|Briefly described|p1|||Max Thickness: 80m||||||
35672|Kanowna Belle Porphyry|60514|6|Mentioned|p47, p48 Fig. 2|Archean|Archean|Age: 2655 Ma. Geological Province: Yilgarn Craton.||||||07-FEB-11
35672|Kanowna Belle Porphyry|60625|5|Briefly described|p47, p48 Figs. 1, 2|Archean|Archean|Age: 2655 Ma. Quatz-feldspar porphyry. Geological Province: Eastern Goldfields.||||||07-NOV-08
35672|Kanowna Belle Porphyry|65834|6|Mentioned|p36|||Kanowna Belle gold mine, Boorara Domain, Kalgoorlie Terrane. Mine terminology.||||Intrudes Graves Dam Grits, Lowes Sandstone, Cemetery and Golden Valley Conglomerates, and QED Rudite.|Feldspar-phyric to aphyric porphyry.|
35672|Kanowna Belle Porphyry|70482|6|Mentioned|p319, 323-329|Archean|Archean|Boorara Domain, Kanowna area, Eastern Goldfields Superterrane, Eastern Yilgarn Craton. Another age of 2656 +/- 6 Ma, also by Ross et al. (2004), is also given. Same ""chemical clan"" as Red Hill Granite. Hosts at least 70% of known mineralisation at the world-class Kanowna Belle Au deposit. Derived from a water-rich metasomatised mantle source. On p319 there appears a Kanowna Belle Suite and a Kanowna Belle Porphyry Supersuite: neither has any apparent justification for promotion of rank and further misuse of such invalid names is strongly discouraged.|2649 +/- 4 Ma (Ross et al., 2004).||||Felsic intrusion. Underwent brittle-ductile sinistral shearing failure causing carbonate brecciation and stockworks, and siliceous breccias; all hosting mineralisation.|
35672|Kanowna Belle Porphyry|73238|5|Briefly described|p21|||The primary host to gold mineralisation at Kanowna Belle.|2649 +/- 4 Ma (Ross et al., 2004).|||||
35672|Kanowna Belle Porphyry|73391|5|Briefly described|p26, 194, 197, 200, 226-229, 241, 244|Archaean|Archaean|See also p304, 416-417. Boorara Domain, Kalgoorlie Terrane. Important host (~5 million ounces) to gold mineralisation. Intruded along the Fitzroy Fault. An ?earlier age determination is 2655 +/- 6 Ma. Appears as KB porphyry on p26.|2661 +/- 8 Ma (SHRIMP: Tripp, 2019).||||Sericite-albite-carbonate altered quartz-hornblende-feldspar porphyry.|
77080|Kantie Murdana Volcanics Member|67129|6|Mentioned|p18 fig 19|Archean|Archean|Murchison Domain, Youanmi Terrane. Appears on diagram as K-M Volcanics Member.||Yaloginda Formation||||07-SEP-17
77080|Kantie Murdana Volcanics Member|68287|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Meta banded chert with centimetre-scale banding shown as c. 2813 Ma. |~ 2813-2820 Ma|Of the Yaloginda Formation.|Informally subdivided into 7 unnamed units.||Meta banded chert; foliated meta banded iron-formation with recrystallized magnetite crystals; felsic volcanic + sedimentary rocks; quartz-feldspar porphyritic rock, metamorphosed; felsic tuff + tuffaceous rock, rhyolite to dacite with phenocrysts.|
77080|Kantie Murdana Volcanics Member|68519|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c.2813 Ma|Unit in Yaloginda Formation.|||Foliated meta banded iron-formation; rhyolitic felsic schist; felsic tuff and tuffaceous rock; rhyolitic to rhyodacitic breccia and tuff.|
77080|Kantie Murdana Volcanics Member|68561|5|Briefly described|GEOL_LUT_CSV folder + GEOCHRON files|||GeologyL_LUT.csv, 100K_INTERPGEOL_LUT.csv||Yaloginda Formation|||Rhyolitic to rhyodacitic breccia and tuff; meta banded chert; foliated meta banded iron-formation.|23-OCT-15
77080|Kantie Murdana Volcanics Member|69583|4|Described|p49, p54, p56-57, p97, p99, p101, p103|Mesoarchean|Mesoarchean|See also p105, p108-111, p178; Plate 2. Nelson (2001). Murchison Domain. Appears as Kantie Murdanna Volcanics Member on p49. Folded on a 500m scale. Seismic interpretation.|2813 +/- 3 Ma (Nelson, 2001).|Yaloginda Formation.||Overlies Windimurra Igneous Complex.|Rhyolitic and dacitic volcanic and volcaniclastic rocks interbedded with minor BIF; locally strongly deformed and recrystallised; meta banded chert with centimetre-scale banding (mapped separately).|
77080|Kantie Murdana Volcanics Member|70020|5|Briefly described|p117,123,126,128|||Geological province: Murchison Domain, Yilgarn Craton. Felsic volcanics coeval with Yaloginda Formation. Associated with VHMS mineralization and are display prospective geochemical characteristics.||||||
77080|Kantie Murdana Volcanics Member|70419|5|Briefly described|p1-4, p7, p9-15, p17, p19-26|Mesoarchean|Mesoarchean|About 0.5 km thick. Magnetitites of the upper zone host several economic vanadium deposits. Shows tight folding on a 500m scale.|2813 +/- 3 Ma (Nelson, 2001).|Yaloginda Formation.||Overlies and is intruded by the Windimurra Igneous Complex.|Rhyolitic volcanics.|
77080|Kantie Murdana Volcanics Member|70796|5|Briefly described|100k_geologyl_lut.csv|Neoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 169003.1.pdf, 194747.1.pdf, 194751.1.pdf, Challa100_2541_stratig.pdf, Windimurra100_2641_stratig.pdf, Wynyangoo100_2542_stratig.pdf. Numerous additional lithologies are discussed.|ca 2813 Ma (inferred)|Yaloginda Formation|||Metamorphosed banded chert; Foliated metamorphosed banded ironformation; Rhyolitic to rhyodacitic breccia and tuff; massive to poorly bedded.|
77080|Kantie Murdana Volcanics Member|70830|5|Briefly described|p26, p30-p31, p33, p38, p40|Mesoarchean|Mesoarchean|Youanmi Terrane.|2813 +/- 3 Ma (Nelson, 2001)|||Overlies and is intruded by the Windimurra Igneous Complex.|Rhyolites.|
77080|Kantie Murdana Volcanics Member|71168|4|Described|p7-p8, p18, p43, p51|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Hosts significant VMS mineralization.|c. 2810 Ma|Yaloginda Formation||Overlies the Murrouli Basalt and the Windimurra and Narndee Igneous Complexes. Overlain by the Coodardy and Mougooderra Formations (Polelle Group).|Felsic volcaniclastic and volcanic rocks.|
77080|Kantie Murdana Volcanics Member|71269|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). Sample GSWA 169003 (vesicular rhyolite) yielded a weighted mean 207Pb/206Pb date of 2813+\-3 Ma. interpreted to be age of igneous crystallisation. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeol_lut.csv.|2813+\-3 Ma (isotopic)|Unit of Yaloginda Formation.|||Psammitic and pelitic schist with abundant cordierite poikiloblasts; quartz-feldspar porphyritic rock; weak to schistose foliation; metamorphosed, felsic tuff and tuffaceous rock; finely banded; fine to medium grained; locally crystal-rich.|
77080|Kantie Murdana Volcanics Member|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Youanmi Terrane.||Yaloginda Formation|||Rhyolitic and dacitic volcanic and volcaniclastic rocks interbedded with minor metamorphosed banded iron-formation; locally strongly deformed and recrystallized.|
77229|Kapi-Parra suite|66256|5|Briefly described|p18 Fig.14, p23 Fig.20, see comments|Stenian|Stenian|Age: late Musgravian. Walpa Pulka Zone. Geochemistry provided. Age: Whole rock Nd isotopic data. See also p24-31, p34-38, p41, p54 App.1, p62 App.3, p71 App.4.|1180 +/- 4 Ma (SHRIMP: GSWA).|Pitjantjatjara Supersuite|||Granite.|11-JAN-17
77229|Kapi-Parra suite|67375|6|Mentioned|p25 Fig.17, p26 Fig.19. |Mesoproterozoic|Mesoproterozoic|A-type. Within-plate, Yb-enriched granite. Late Musgrave Orogeny.||Unit in Pitjantjatjara Supersuite.||||
77229|Kapi-Parra suite|67553|6|Mentioned|p27-28,33,67|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province, North Australian Craton. Late Musgravian granite.||Unit of Pitjantjatjara Supersuite.||||
77229|Kapi-Parra suite|69091|6|Mentioned|p64 Fig.4.10|||Late Musgravian granite.||Pitjantjatjara Supersuite|||Granite.|26-SEP-14
77229|Kapi-Parra suite|69729|5|Briefly described|p74 Fig.7, p77-78|||Geochemistry plots.||Pitjantjatjara Supersuite.|||A-type granites.|
24332|Karalundi Formation|7161|5|Briefly described|p92 Fig.4, p93-4|||Neds Creek Basin. Less than 1900m thick (from p92 Fig.4).||||Underlain by the Doolgunna Formation. Overlain by the Narracoota Volcanics.|Upward-coarsening sedimentation units of laminated mudrock and sandstone that resemble delta-front facies.|
24332|Karalundi Formation|12099|4|Described|p680-1, p677-8 Figs.2 & 4, p682 Fig.7|Paleoproterozoic|Paleoproterozoic|Included in Glengarry Group by Gee (1987). Also contains jasperoidal chert interpreted to be fumarolic pipes (Gee, 1979, 1987). Max thickness of ~2.5km. Outcrops in a northeast-trending belt along the southeastern margin of the Bryah Basin.||Basal unit in Bryah Group.||Overlies Maraloou Formation. In fault contact with the Doolgunna Formation in the southeast and east of the Bryah Basin; intercalated with Narracoota Formation in the south.|Characterised by immature clastic units containing angular quartz and lithic fragments in a sericite-clay-rich matrix; conglomerate, siltstone, calcareous siltstone, cross-bedded arenite, ferruginous arenite, litharenite, minor dolomite and shale.|04-MAR-13
24332|Karalundi Formation|22493|6|Mentioned|p93|||||||||
24332|Karalundi Formation|22940|4|Described|p11, Fig.1 p3|Paleoproterozoic|Paleoproterozoic|See also Fig.6 p14. of Bryah Group.||||||07-NOV-08
24332|Karalundi Formation|23593|5|Briefly described|p2 Fig 1|||Of Bryah Group. Geological Province: Bryah Basin||||||
24332|Karalundi Formation|23600|5|Briefly described|p4 Fig 2|||Of Bryah Group. Bryah Basin.||||||
24332|Karalundi Formation|23744|6|Mentioned|p2 Fig 1|||Of Bryah Group. Geological Province: Bryah Basin.||||||
24332|Karalundi Formation|23747|4|Described|p9|Paleoproterozoic|Paleoproterozoic|See also page 4 table 1. Of Bryah Group. Geological Province: Bryah Basin.||||||07-NOV-08
24332|Karalundi Formation|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Bryah Group. Geological Province: Bryah Basin||||||
24332|Karalundi Formation|23749|4|Described|p11|Proterozoic|Proterozoic|Of Bryah Group. Geological Province: Bryah Basin.||||||
24332|Karalundi Formation|23750|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Bryah Group. Geological Province: Bryah Basin.||||||
24332|Karalundi Formation|23890|5|Briefly described|p21 Fig.11|||Of Bryah Group. Geological Province: Bryah Basin.||||||
24332|Karalundi Formation|24021|5|Briefly described|p3, Fig. 1|||Parent: Bryah Group||||||
24332|Karalundi Formation|35975|3|Fully described|p102|||||||||
24332|Karalundi Formation|38994|6|Mentioned|p31|||||||||
24332|Karalundi Formation|40297|6|Mentioned|p109|||||||||
24332|Karalundi Formation|40937|6|Mentioned|p28|||||||||
24332|Karalundi Formation|40938|5|Briefly described|p11|||Mention P69 and Fig.5||||||
24332|Karalundi Formation|40989|4|Described|p20|||||||||
24332|Karalundi Formation|42260|6|Mentioned|p125|||||||||
24332|Karalundi Formation|43069|5|Briefly described|p18|||of Glengarry Group||||||
24332|Karalundi Formation|44204|5|Briefly described|Map Legend||Proterozoic|||||||
24332|Karalundi Formation|49893|6|Mentioned|p2 Fig.1|||Of the Bryah Group.||||||
24332|Karalundi Formation|49896|5|Briefly described|p2 Tb. 1|||Of Gee (1979a). Of the Bryah Group.||||||
24332|Karalundi Formation|50222|4|Described|p320 Fig. 3, p324|Paleoproterozoic|Paleoproterozoic|Basal unit of the Bryah Group.  Age: >2.1Ga and 2.7Ga (latter are detrital zircons from Archaean source indicating a diverse provenance).  Max. thickness: ~2500m.  Geological Province: Bryah Basin.||||||07-NOV-08
24332|Karalundi Formation|50226|5|Briefly described|p420, p421 Fig. 4|||Of the Bryah Group.  Characterised by immature clastic sedimentary rocks.  Geological Province: Bryah Basin.||||||
24332|Karalundi Formation|61271|5|Briefly described|p104|||Of the Bryah Group. Overlain by the Narracoota Formation. Consists of greywacke and conglomerate.||||||27-MAY-06
24332|Karalundi Formation|62289|5|Briefly described|plate 1, p3 Fig. 1, p4 Fig. 2|Palaeoproterozoic|Palaeoproterozoic|Of Bryah Group; sandstone; minor shale and conglomerate; metamorphosed; Geol. Prov: Bryah Basin.||||||
24332|Karalundi Formation|63866|5|Briefly described|p164|||Western Glengarry Basin.||Bryah Group||||
24332|Karalundi Formation|64384|5|Briefly described|p78 Tb. 8|||Of the Glengarry Group. Geological province: Glengarry Sub-basin.||||||07-FEB-11
24332|Karalundi Formation|64580|4|Described|map legend||Paleoproterozoic|Of Bryah Group. Ferruginous, chloritic shale and quartz-feldspar wacke; partly manganiferous and calcareous; includes iron formation and chert; metamorphosed.||||||09-DEC-08
24332|Karalundi Formation|65408|5|Briefly described|pp82-83.|Paleoproterozoic|Paleoproterozoic|||Unit in Bryah Group.|||Sequence of greywacke and conglomerate.|21-JAN-22
24332|Karalundi Formation|65411|5|Briefly described|p88, p90.|Paleoproterozoic|Paleoproterozoic|Mis-spelt as Karalindi Formation on p90.||Basal unit in Bryah Group.|||Includes lithic wacke, sublitharenite, shale.|
24332|Karalundi Formation|65412|5|Briefly described|p97 Fig.1.|Paleoproterozoic|Paleoproterozoic|Rift-shoulder lithologies.||Basal unit in Bryah Group.||Intercalated with Narracoota Formation.|Basal clastic sequence.|
24332|Karalundi Formation|65419|1|Redefined|p4 Fig.1, p27, pp30-32, p49.|Paleoproterozoic|Paleoproterozoic|Type area along the E-W fence line, 11 km NNW of Karalundi. Up to 2.5 km thick in places. Essentially as defined by Gee (1979) but with some redistribution and addition of outcrops; corresponds in part with the 'Shale and wacke unit' of Elias et al. (1982). Transferred now from Glengarry Group (Gee, 1979; Gee and Grey, 1993) to Bryah Group: the type area lies within the outcrop of the Bryah Group. Some deposition may have been coeval with Narracoota Formation basalts.||Unit in Bryah Group.||In faulted contact with Peak Hill Schist, Juderina and Doolgunna Formations. Is overlain by, and interfingers with, Narracoota Formation. Is overlain unconformably by Mount Leake Formation.|Shale, ferruginous quartz arenite with quartz-pebble conglomerate, some arkosic and chert lenses, and chert breccia; local sublitharenite, minor black shale, and purple-grey shale; conglomeratic lenses common within the shales.|
24332|Karalundi Formation|65913|6|Mentioned|p2 Fig.1. |Paleoproterozoic|Paleoproterozoic|||Unit in Bryah Group.||||
24332|Karalundi Formation|66427|6|Mentioned|p72 Fig.26|||||||||
24332|Karalundi Formation|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic|Bryah Basin||Bryah Group|||Sandstone; minor shale and conglomerate|
24332|Karalundi Formation|69003|5|Briefly described|p11-12|||Bryah Basin. c.2500m thick.||Bryah Group.||Is overlain by Narracoota Formation.||
24332|Karalundi Formation|69166|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|||Bryah Group|||Sandstone; minor shale and conglomerate.|
24332|Karalundi Formation|69596|6|Mentioned|p10-11|||Bryah Basin.|||||Siliciclastic rocks.|
24332|Karalundi Formation|70795|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic||2014-1920 Ma||||Sandstone; minor shale and conglomerate.|
24332|Karalundi Formation|70796|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|Bryah Basin, Capricorn Orogen. See also glengarry_100k_geologyp_lut.csv, glengarry_500k_interpgeop_lut.csv, Glengarry100_2645_stratig.pdf.|2014  1920 Ma (inferred)|Bryah Group, upper|||Sandstone; minor shale and conglomerate.|
24332|Karalundi Formation|70804|4|Described|p2, p6-p7, p9, p24, p26|||Outcrops in a northeasterly trending belt along the southeastern margin of the Bryah Basin. Estimated to reach a maximum thickness of 2500m. See also p31, p37-p38, p43, p47, plate 1.||Basal Bryah Group||Faulted against the Doolgunna Formation. Overlain by the Narracoota Formation.|Quartz-lithic wacke and conglomerate, siltstone, calcareous siltstone, cross-bedded arenite, ferruginous arenite, litharenite, dolomite and shale.|
24332|Karalundi Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, conglomerate, chert, shale|
24332|Karalundi Formation|71269|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen, West Australian Craton. Of Bryah Basin. Events: Capricorn Orogeny (1817-1772 Ma); Glenburgh Orogeny (2002-1947 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, glengarry_100k_geologyp_lut.csv, glengarry_500k_interpgeop_lut.csv.|2014-1920 Ma (inferred)|Unit of Bryah Group.|||Sandstone; minor shale and conglomerate|
24332|Karalundi Formation|71468|4|Described|p24-26,28,30-36,38|Orosirian|Orosirian|Geological province: Capricorn Orogen, Yilgarn Craton. Of Bryah Sub-basin. Basal unit of the Bryah Sub-basin, formed in a nascent rift setting (Occhipinti et al., 2017; Pirajno et al., 2016). Age is constrained to 2030-1990 Ma, primarily from the DeGrussa VHMS deposit. Differentiated plagiogranites in the Karalundi Formation from DeGrussa and in an unmineralised drillhole to the west of DeGrussa gave zircon U-Pb ages of 2014+\-7 Ma and 2018+\-9 Ma, respectively. Negative Nb anomalies suggest crustal input in either a suprasubduction zone or intracontinental rift setting (Baier et al., 2008; Pearce, 2008); most likely a continental rift origin for the Bryah Sub-basin; which is consistent with the northern Yilgarn Craton being a passive margin prior to collision with the Pilbara Craton-Glenburgh Terrane at 1965-1950 Ma.||Bryah Group|Includes the Noonyereena Member.|Overlain by, and interfingers with Narracoota Formation. Unconformably overlies the Trillbar Complex.|Siliciclastic rocks, massive basalt flows, pillow basalt, hyaloclastite, volcaniclastic rocks and jaspilite.|20-AUG-19
24332|Karalundi Formation|71484|4|Described|p122-123,125-128,134,137,139|Orosirian|Orosirian|Geological province:  Of Bryah Basin. Contains voluminous volcanosedimentary and siliciclastic sedimentary rocks dissimilar to continental flood basalts, and more likely formed in a continental rift setting (Ernst, 2014). Maximum depositional age of 2045+\-16 Ma (SHRIMP; Wingate et al., 2014a,b). Hawke et al. (2014) also provided Re-Os dates of 2027+\-7 Ma and 2011+\-7 Ma from VMS mineralisation from within the Karalundi Formation at the DeGrussa Cu-Au deposit. Intuded by granodiorite with SHRIMP ages c. 2014+\-7 Ma and 2018+\-9 Ma.|c. 2030-2010 Ma|Unit of Bryah Group.||Basal unit of Bryah Group. Overlain by, and grades basinward to Narracoota Formation.|Basaltic volcanics, or andesitic basalt intercalated with sandstone; lithic wacke, minor shale, conglomerate, local mafic volcanics.|30-AUG-19
24332|Karalundi Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Bryah Basin.||Bryah Group, lower|||Sandstone; minor shale and conglomerate.|
74832|Karbar Monzogranite|64891|5|Briefly described|p37 Fig. 2, p52-53 Tb. 1|Archean|Archean|Of the Tuckanarra Suite. Age: c. 2670Ma. Geological province: Murchison Domain. Monzogranite; metmorphosed.||||||07-FEB-11
74832|Karbar Monzogranite|67129|5|Briefly described|p19 Fig.20|Archean|Archean|Murchison Domain, Youanmi Terrane.||Tuckanarra Suite.|||Monzogranite.|
74832|Karbar Monzogranite|69583|6|Mentioned|p52|||Murchison Domain.||||||
74832|Karbar Monzogranite|70796|5|Briefly described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_interpgeop_lut.csv., 500k_interpgeop_lut.csv.|ca 2690  2665 Ma (inferred)|Tuckanarra Suite|||Monzogranite; weak solidstate overprint, generally increasing towards pluton margins; metamorphosed|
74832|Karbar Monzogranite|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.|2697-2665 Ma (inferred)|Unit of Tuckanarra Suite.|||Monzogranite; weak solid-state overprint, generally increasing towards pluton margins; metamorphosed|
22066|Kardinya Shale Member|12759|2|Defined|p39; p28 Tb. 7; p32 Fig 15; P36 Fig 17|Cenomanian|Albian|Named from: Kardinya suburb, S of Perth. Type Section: Bore AM42 at AMG Zone 50 (387984m E, 6452223m N), 28-167 m depth (max 140 m). Confining bed for aquifers.||Of Osborne Formation.||Overlain conformably by Mirrabooka Member or unconformably by Molecap Greensand or Gingin Chalk. Underlain by Henley Sandstone Member (conformably) or the Wanneroo or Pinjar Members (unconformably).|Moderately to tightly consolidated, interbedded siltstones and shales, dark green to black, often puggy, glauconitic, and contain thin interbeds of mostly fine-grained sandstone.|12-MAY-14
22066|Kardinya Shale Member|14227|5|Briefly described|Enclos. 2|Cretaceous|Cretaceous|Of Coolyena Group. Probably of Osborne Formation. Presented as Kardinya Sh Mem.||||||07-FEB-11
22066|Kardinya Shale Member|67115|6|Mentioned|p64, p65 Fig. 3 |Cretaceous|Cretaceous|||Osborne Formation||Overlies the Pinjar Member (Leederville Formation).|Siltstone/shale.|
22066|Kardinya Shale Member|68254|6|Mentioned|p1046 Tb.4, p1040 Tb.3|||Member status specified in column heading of Table 3. See informal Kardinya Shale in this paper.||||||
22066|Kardinya Shale Member|70099|5|Briefly described|p6|Cenomanian|Albian|Southern Perth Basin. Correlated to Mentelle 7B Supersequence.||Osborne Formation.||||
80949|Karijini Dolerite|71808|4|Described|ix, p8-p9, p45|Proterozoic|Neoarchean|Hamersley Province. Dolerite is well exposed under several metres thickness of Roy Hill Shale Member in the Alligator and Weeli Wolli anticlines. See also p48, p77, p92, p117, p234. Map symbol PKd implies Proterozoic age, but the dolerite intrudes Neoarchean units.||||Intrudes the Jeerinah Formation, Nammuldi Member.|Medium to dark green, fine to medium-grained, locally microporphyritic dolerite and diorite.|27-APR-19
80171|Karlaya Member|71211|4|Described|ii, p21, p26, p27 fig 2.3, p28-p30|Mesoproterozoic|Mesoproterozoic|Less than or equal to 100m thick.  Ignimbrites are characterised by rheomorphism and lava-like behaviour. See also p37, p38, p50-p54, p57, p59-p61, p67, p68, p86-p88, p137 fig 4.2, p138, p182, p208, p265-p266, p269. ||Kathleen Ignimbrite||Conformably overlies the Kurrparu Member. Overlain by the Kilykilykarri Member.|Vitriclastic, rhyolitic ignimbrites, breccias and lapilli-tuff facies.|03-OCT-17
31690|Karratha Granodiorite|22449|6|Mentioned|Table3 P27||Archean|Age of unit is 3260 Ma||||||07-NOV-08
31690|Karratha Granodiorite|22471|6|Mentioned|25|Archean|Archean|Geol province Pilbara||||||07-NOV-08
31690|Karratha Granodiorite|23046|5|Briefly described|174|||||||||
31690|Karratha Granodiorite|23244|6|Mentioned|p14||Archean|Intruded the base of the greenstones at 3261+/-4Ma.||||||07-NOV-08
31690|Karratha Granodiorite|23484|4|Described|p16|Archean|Archean|Age: 3270-3250Ma.  Intrudes the Roebourne Group.||||||07-NOV-08
31690|Karratha Granodiorite|23783|5|Briefly described|p36|Archean|Archean|||||||07-NOV-08
31690|Karratha Granodiorite|23784|4|Described|p10|Archean|Archean|Age: 3270Ma.  Intrudes the Roebourne Group.||||||07-NOV-08
31690|Karratha Granodiorite|23789|4|Described|p11|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
31690|Karratha Granodiorite|23793|4|Described|p31|Archean|Archean|Age: c. 3270-3260Ma. Ranges in composition from tonalite to granodiorite||||||07-NOV-08
31690|Karratha Granodiorite|23794|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
31690|Karratha Granodiorite|23813|5|Briefly described|p89|Archean|Archean|Age: ca.3260Ma.  Intrudes the Roebourne Group.  Geological Province: Pilbara Craton.||||||07-NOV-08
31690|Karratha Granodiorite|24023|4|Described|p22|Archean|Archean|||||||07-NOV-08
31690|Karratha Granodiorite|24024|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
31690|Karratha Granodiorite|24184|4|Described|p710, 712|Archean|Archean|Geological Province: Pilbara Craton. Age: ca. 3270-3250Ma, synchronous with Roebourne Group||||||11-DEC-08
31690|Karratha Granodiorite|24541|4|Described|p1, p12, p29|Archean|Archean|Geological Province: West Pilbara Granite-Greenstone Terrane. Age: c. 3270 - 3260 Ma.||||||07-NOV-08
31690|Karratha Granodiorite|24543|5|Briefly described|Map legend|Archean|Archean|Age: c.3270-3260Ma.  Granodiorite and tonalite; foliated with local compositional banding.||||||07-NOV-08
31690|Karratha Granodiorite|24550|5|Briefly described|p41, p76|Archean|Archean|See also Karratha Granitoid. Intrudes Ruth Well Formation (Roebourne Group). Age: 3265Ma (Nelson 1998b; Smith et al 1998). Geological Province: Pilbara Craton. See also p78 Fig. 5.2, p105, p191.||||||07-FEB-11
31690|Karratha Granodiorite|43822|5|Briefly described|map legend|Archean|Archean|Age approx. 3260 Ma.||||||07-NOV-08
31690|Karratha Granodiorite|50430|4|Described|p159 Fig.2||Archean|Age: 3270-3260 Ma. In West Pilbara Granite-Greenstone Terrane.||||||04-DEC-08
31690|Karratha Granodiorite|61253|5|Briefly described|p56|Archean|Archean|Together with the Roebourne Group units (in West Pilbara granite-Greenstone Terrane) interpreted to be a rifted segment of Sulphur Springs Group/Cleland Supersuite of the East Pilbara Granit-Greenstone Terrane. Age: 3.27Ga.   Geol.Prov: Pilbara Craton.||||||07-NOV-08
31690|Karratha Granodiorite|61267|5|Briefly described|p71, p73 Tb.1|Archean|Archean|Age: c. 3270 Ma. Intrudes rocks of the Roebourne Group. Hornblende trondhjemite; biotite granite. Geological Province: Pilbara Craton.||||||07-NOV-08
31690|Karratha Granodiorite|63441|5|Briefly described|p2, p9 Tb. 2|Archean|Archean|Of the Cleland Supersuite. Ages: from 3270+/-2Ma to 3261+/-4Ma. Geological province: West Pilbrara Superterrane/Pilbara Craton. Formerly referred to as the Karratha Batholith.||||||07-FEB-11
31690|Karratha Granodiorite|63538|4|Described|p2 Fig. 1, p5, p29|Archean|Archean|Overlain by Regal Formation. Contemporaneous with Roebourne Group. Age: 3270 Ma. Geological Province: Pilbara Craton.||||||17-APR-13
31690|Karratha Granodiorite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Cleland Supersuite.  Age: 3270-3261Ma. Geological province: Karratha Terrane, West Pilbara Superterrane.granodiorite and tonalite; foliated with local compositional banding; metamorphosed.||||||11-DEC-08
31690|Karratha Granodiorite|64580|4|Described|map legend|Paleoarchean|Paleoarchean|Of Cleland Supersuite. Granodiorite and tonalite; foliated with local compositional banding; metamorphosed.||||||15-DEC-08
31690|Karratha Granodiorite|64632|6|Mentioned|p201 Fig.1|Paleoarchean|Paleoarchean|Karratha Terrane (3.27-3.25 Ga), West Pilbara Superterrane||||||
31690|Karratha Granodiorite|66118|6|Mentioned|p146 Fig.1|||Pilbara Craton. West Pilbara Superterrane. Karratha Terrane.|3260 Ma|||||
31690|Karratha Granodiorite|66217|5|Briefly described|p34.|Paleoarchean|Paleoarchean|Karratha Terrane.|c.3265 Ma.|Unit in Cleland Supersuite.||||
31690|Karratha Granodiorite|67201|4|Described|p11, p13 Fig.8, p14, see comments|||Pilbara Craton, West Pilbara Superterrane, Karratha Terrane, Prinsep Dome. Much older Nd model ages indicate magma generation involved older crust or enriched lithospheric mantle. Page location continued: p25-26, p37-39, p43, p69.|3270 Ma U-Pb SHRIMP; 3480 Nd TDM model age|Cleland Supersuite||Intrudes Ruth Well Formation. Is unconformably overlain by Nickol River Formation.|Tonalite and granodiorite; foliated with local compositional banding; metamorphosed.|24-NOV-16
31690|Karratha Granodiorite|68035|5|Briefly described|p289, p290 Fig 5|Paleoarchean|Paleoarchean|Karratha Terrane, NW Pilbara. Nd TDM model ages of 3.48 - 3.43 Ga indicate that magma generation involved older crust or enriched lithospheric mantle (Sun and Hickman, 1998).|3270 - 3260 Ma|||||
31690|Karratha Granodiorite|69185|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: West Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 3270 Ma|Unit of Cleland Supersuite.|||Granodiorite and tonalite; foliated with local compositional banding; metamorphosed|
31690|Karratha Granodiorite|69301|4|Described|p11-12|||Pilbara Craton. West Pilbara Superterrane. Karratha Terrane. Nd TDM model age (approximate time when source material was extracted from depleted mantle) of 3.48-3.43 Ga (Sun & Hickman 1998) indicates that magma generation involved older crust or enriched lithospheric mantle.|see comments|||Intrudes Ruth Well Formation.|Includes tonalite and granodiorite.|
31690|Karratha Granodiorite|70022|6|Mentioned|p114|||Karratha Terrane, West Pilbara Superterrane.|3265 Ma.|||||
31690|Karratha Granodiorite|70775|4|Described|iv, p10, p12-p13, p15-p17|Paleoarchean|Paleoarchean|Karratha Terrane. Isotopic evidence suggests this unit was derived from partial melting of c. 3500 Ma crust or enriched lithospheric mantle. The type area is immediately south of Karratha. A metamorphic event at 3160 +/- 158 Ma is interpreted by Kiyokawa (1993). Interpreted to have been the product of a mantle plume. See also p19-p20, p22-p26, p29, p39, p49, p63, p68-p69, p80-p81, p94, p100.|c. 3270-3261 Ma|Cleland Supersuite||Intrudes the Roebourne Group and the Ruth Well Formation. Intruded by the Andover Intrusion. Unconformably overlain by the Nickol River Formation.|Granodiorite and tonalite; folaited with local compositiona; banding; metamorphosed.|
31690|Karratha Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite, tonalite|
31690|Karratha Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||Max age 3270+/-2 Ma, 3261+/-4 Ma.|Cleland Supersuite|||Granodiorite and tonalite; foliated with local compositional banding; metamorphosed.|
31690|Karratha Granodiorite|72251|5|Briefly described|p52|Paleoarchean|Paleoarchean|Geological province: Karratha Terrane, West Pilbara Superterrane, Pilbara Craton.|3265 Ma|||||
31690|Karratha Granodiorite|72668|6|Mentioned|p3, p12, p28|||Karratha Terrane of the West Pilbara Superterrane. Contemporaneous with the Roebourne Group.|c. 3490 Ma (Nd)||||Subvolcanic intrusions.|13-JAN-22
33195|Karri Karri Member|23529|4|Described|p17|Paleoproterozoic|Paleoproterozoic|Formerly included in the Wandiwarra Formation. Parent: Chiall Formation. Max. thickness: 500-1000m. Geological Province: Earaheedy Basin.||||||24-JUN-09
33195|Karri Karri Member|23530|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Chiall Formation, Earaheedy Basin||||||07-NOV-08
33195|Karri Karri Member|23589|4|Described|p28|||Was the lower part of the Wandiwarra Formation. Of Windidda Formation. Overlying unit Chiall Formation. Underlying unit Frere Formation. Earaheedy Basin.||||||
33195|Karri Karri Member|23611|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|See also page 33 Appendix 1.  Of Chiall Formation. Geological Province: Earaheedy Basin.||||||07-NOV-08
33195|Karri Karri Member|24017|4|Described|p18|Paleoproterozoic|Paleoproterozoic|Of the Chiall Formation. Geological Province: Earaheedy Basin.||||||07-NOV-08
33195|Karri Karri Member|24018|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Windidda Formation, Earaheedy Group.  Geological Province: Earaheedy Basin.||||||07-NOV-08
33195|Karri Karri Member|24578|5|Briefly described|p778 Fig.3|Paleoproterozoic|Paleoproterozoic|Of the Chiall Formation. Geological Province: Earaheedy Basin||||||07-NOV-08
33195|Karri Karri Member|50188|2|Defined|p7, p4, Fig. 2|Paleoproterozoic|Paleoproterozoic|Basal unit of the Chiall Formation. Formerly assigned to the underlying Windidda Fm. Max.thickness: 1000m. Conformably overlies Frere Formation. Laminated ferruginous shale and siltstone. See also p3.||||||07-NOV-08
33195|Karri Karri Member|50195|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Chiall Formation.  Geological Province: Earaheedy Basin.||||||07-NOV-08
33195|Karri Karri Member|50222|5|Briefly described|p320 Fig.3, p329|Paleoproterozoic|Paleoproterozoic|Of the Chiall Formation (Miningarra Subgroup, Earaheedy group).  Thick succession of shale, siltstone and mudstone.  Geological Province: Earaheedy Basin.||||||07-NOV-08
33195|Karri Karri Member|50223|5|Briefly described|p345 Fig.2, p346|Paleoproterozoic|Paleoproterozoic|Basal distal part of the Chiall Formation. Thinly laminated shale. Overlies the Frere and Windidda Formations. Max. thickness: 300m. Geological Province: Earaheedy Basin.||||||07-NOV-08
33195|Karri Karri Member|50309|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Earaheedy Basin. Of the Chiall Formation which overlies it. Overlies: Frere Formation, Windidda Formation.||||||07-NOV-08
33195|Karri Karri Member|50319|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Chiall Formation (Miningarra Subgroup). Geological Province: Earaheedy Basin.  Shale, generally finely laminated, siltstone, and minor sandstone, deformed and metamorphosed in the Stanley Fold Belt.||||||07-NOV-08
33195|Karri Karri Member|50334|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Chiall Formation (Miningarra Subgroup). Geological Province: Earaheedy Basin||||||07-NOV-08
33195|Karri Karri Member|50626|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Windidda Formation (Earaheedy Group).  Siltstone and shale.  Geological Province: Earaheedy Basin.||||||07-NOV-08
33195|Karri Karri Member|64284|4|Described|p59-60|Paleoproterozoic|Paleoproterozoic|Of Chiall Formation (Minningarra Subgroup). Formerly part of the former Wandiwarra Formation. Geological Province: Earaheedy Basin. Shale,siltstone.||||||07-FEB-11
33195|Karri Karri Member|64285|5|Briefly described|p66 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Chaill Formation - created as a result of revision of the Earaheedy Group. Includes steeply dipping shale units.||||||06-MAR-14
33195|Karri Karri Member|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Of Chiall Formation. Shaly siltstone.||||||15-DEC-08
33195|Karri Karri Member|64772|5|Briefly described|p10 Fig. 5, Plate 1, p30|Paleoproterozoic|Paleoproterozoic|Base of Chiall Formation (Earaheedy Group). Previously of the former (underlying) Windidda Formation. Geological province: Earaheedy Basin. Shale units host manganese mineralisation related to structurally controlled hydrothermal veins containing quartz¿iron¿manganese oxides. See also p12, p18 Fig.8, p25 Fig.11, p31 Fig.18, p32 Fig.20, p33 Fig.21, p36, p39 Fig.25-26, Plate 1|||||Thick succession of shale, siltstone, and mudstone|25-NOV-13
33195|Karri Karri Member|65264|5|Briefly described|p27, p44 Appdx. 1|Paleoproterozoic|Paleoproterozoic|Of Chiall Formation (Mooloogool [??] Subgroup). Overlain by Wandiwarra Member. Geological province: Earaheedy Basin. Comprises shale and siltstone.||||||06-MAR-14
33195|Karri Karri Member|65472|6|Mentioned|p3 Fig.2|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin.||Of Chiall Formation.||||24-SEP-15
33195|Karri Karri Member|65692|6|Mentioned|p55-56|||||Chiall Formation.||||
33195|Karri Karri Member|66427|5|Briefly described|p46 Fig.4, p54-55, p59, p63-64|||First mapped as part of Windidda Formation, but later work saw re-interpretation as part of Chiall Formation.||Of the Chiall Formation.||Conformably overlies Frere Formation. Is overlain conformably (transitionally) by Wandiwarra Member.|Contains a thick succession of shale, siltstone and mudstone. Maximum thickness of 600m.|
33195|Karri Karri Member|69003|5|Briefly described|p14 Fig.18|||Earaheedy Basin.||Chiall Formation.||Unconformably overlies Windidda Member (Frere Formation).||
33195|Karri Karri Member|69152|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin||Of Chiall Formation|||Shaly siltstone.|24-SEP-15
33195|Karri Karri Member|69313|5|Briefly described|p25 Fig.4.3|||||Chiall Formation||Overlain by the Wandiwarra Member. Overlies the Windidda Member (Frere Formation).|Mudstone.|08-SEP-17
33195|Karri Karri Member|69596|6|Mentioned|p10|||Earaheedy Basin.||Chiall Formation.||||
33195|Karri Karri Member|70153|5|Briefly described|100k_geologyp10_lut.csv|Paleoproterozoic|Paleoproterozoic|||Chiall Formation|||Shaly siltstone.|
33195|Karri Karri Member|71042|6|Mentioned|p97|||||Chiall Formation||||
33195|Karri Karri Member|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||shale, siltstone, sandstone|
33195|Karri Karri Member|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen. Of Earaheedy Basin. See 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.||Unit of Chiall Formation.|||Shaly siltstone|
35316|Karukali Quartzite|50286|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group.||||||
35316|Karukali Quartzite|50321|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group.||||||28-MAY-04
35316|Karukali Quartzite|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. White crystalline quartz sandstone; rounded quartz pebble conglomerate beds; local heavy mineral layers of hematite and magnetite. Geological Province: Musgrave Block.||||||
35316|Karukali Quartzite|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Tjauwata Group. Geological Province: Musgrave Block.||||||14-JAN-05
35316|Karukali Quartzite|61154|5|Briefly described|p16, p18 Fig. 10|Mesoproterozoic|Mesoproterozoic|Basal unit of Tjauwata Group. Thin succession  of quartzite, quartz-muscovite schist, and quartz pebble to boulder conglomerate overlying the Musgrave basement granite.  Overlain by Tjuninanta Formation. Geological Province: Musgrave Block.||||||
35316|Karukali Quartzite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. White crystalline quartz sandstone, rounded quartz pebble conglomerate beds, local heavy mineral horizons of hematite and magnetite.||||||
35316|Karukali Quartzite|62989|5|Briefly described|p39|Mesoproterozoic|Mesoproterozoic|Basal unit of the Tjauwata Group. Unconformably overlies the Mesoproterozoic granites of the Musgrave Province. Max. thickness: 10m. The quartzite contains heavy mineral assemblages dominated by hematite, quartz muscovite schist and quartz conglomerate.||||||07-FEB-08
35316|Karukali Quartzite|65256|2|Defined|p6 Tb.1, p8-9, p13, p14 Fig 10, p37, p38|Stenian|Stenian|New name. Previously described as the basal rocks of the Mount Harris Basalt. 5-10m thick. Disconformably(?) underlies basal units of Tjauwata Group; correlated with MacDougall Formation (Bentley Supergroup). Intruded by mafic dykes interpreted to belong to Alcurra dolerite. Sediment probably derived from Pottoyu Granite Suite.||Basal unit of Tjauwata Group.||Unconformably overlies Pottoyu Granite Suite, Bloods Range Formation;underlies Mount Harris Basalt; conformably underlies Tjuninanta Formation.|Crystalline quartz sandstone, quartzite and quartz-muscovite schist often rich in hematite and magnetite with minor quartz pebble conglomerate; contains heavy mineral horizons.|19-MAY-14
35316|Karukali Quartzite|68995|6|Mentioned|p6|||||Tjauwata Group||||
35316|Karukali Quartzite|69091|5|Briefly described|p70|||Basal unit of Bentley Supergroup.||Tjauwata Group||Equivalent to MacDougall Formation (of Kunmarnara Group).||26-SEP-14
35316|Karukali Quartzite|69436|5|Briefly described|p21:4, 13-14|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Shoreline deposits.||Basal Tjauwata Group.||Is overlain by Tjuninanta Formation. Lateral equivalent of the MacDougall Formation.|A thin (5-10m thick) succession of quartzite, quartz-muscovite schist, and quartz pebble and boulder conglomerate. Includes lenses of rounded quartz cobble clasts, quartz gravel layers and heavy mineral (mainly haematite) horizons.|12-JUL-16
35316|Karukali Quartzite|69729|5|Briefly described|p79|||Bentley Basin.||Tjauwata Group.||Equivalent to the MacDougall Formation.||
35316|Karukali Quartzite|70018|4|Described|p233,235-236|Mesoproterozoic|Mesoproterozoic|Amadeus Basin. Interbedded siliciclastic sedimentary rocks.||Unit of Tjauwata Group.||Overlain by Tjuninanta Formation.|Quartzite, quartz conglomerate, quartz muscovite schist.|
35316|Karukali Quartzite|71210|6|Mentioned|p8|||||||Equivalent to MacDougall Formation.||
35316|Karukali Quartzite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone|
35316|Karukali Quartzite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Sequence is aboubt 5-10m thick. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Sample GSWA 208466 (micaceous quartzite) yielded a concordia age of 1163+\-13 Ma, interpreted as maximum depositional age of the quartzite. Sample GSWA 208494 (quartzite) yielded a a weighted mean 207Pb/206Pb age of 1177+\-18 Ma, interpreted as maximum depositional age of the sandstone protolith. See 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeol_lut.csv.|1084-1075 Ma (inferred)|Unit of Tjauwata Group.||Basal unit of Tjauwata Group. Underlain by Pitjantjatjara Supersuite. Equivalent to MacDougall Formation.|Quartzite and quartz-muscovite schist; locally rich in hematite and magnetite; minor quartz-pebble conglomerate|
35316|Karukali Quartzite|72094|4|Described|p7, p9, p17||Stenian|Geological province: Petermann Nappe Complex. Maximum depositional age constrained by 1177+/-18 Ma and 1163+/-13Ma ages. Summary table of zircon geochronology on p9 Table 2.||Of Tjauwata Group.||Basal sequence of the Tjauwata Group. Overlain conformably by Mount Harris Basalt. Likely time- and lateral equivalent to the MacDougall Formation.|Includes quartzite (material dated).|
33450|Kavir Granodiorite|23416|5|Briefly described|Map Legend|Archean|Archean|Of Yule Granitoid Complex, Pilbara Craton||||||07-NOV-08
33450|Kavir Granodiorite|23755|5|Briefly described|p54|Archean|Archean|See also page 18 Table 2. Geological Province: Yule Granitoid Complex.||||||07-NOV-08
33450|Kavir Granodiorite|24531|5|Briefly described|p8-9 Fig. 3|Archean|Archean|Of the Yule Granotoid Complex.  See also p25.||||||07-NOV-08
33450|Kavir Granodiorite|24532|5|Briefly described|Map legend|Archean|Archean|Of the Yule Granitoid Complex.  Age: c.3240Ma.||||||07-NOV-08
33450|Kavir Granodiorite|50379|5|Briefly described|Map Legend|Archean|Archean|Of Yule Granitoid Complex. Geological Province: Pilbara Craton. Age: 3420-3235 Ma||||||07-NOV-08
33450|Kavir Granodiorite|63441|5|Briefly described|p9 Tb. 2|Archean|Archean|Of the Cleland Supersuite. Age: c.3240Ma. Geological province: Pilbara Craton.||||||07-FEB-11
33450|Kavir Granodiorite|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Cleland Supersuite. Geological Province: Pilbara Craton. Metomorphosed, biotite granodiorite and minor pegmatitic granite; fine to medium grained; metamorphic foliation.||||||
33450|Kavir Granodiorite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Cleland Supersuite. Meta biotite granodiorite and minor pegmatitic granite; fine- to medium-grained; foliated.||||||
33450|Kavir Granodiorite|68282|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c.3240 Ma|Of the Cleland Supersuite||Sheets and patches are included in Petroglyph Gneiss.|Meta biotite granodiorite and minor pegmatitic granite; fine to medium grained; foliated.|03-DEC-14
33450|Kavir Granodiorite|69013|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane.|c. 3240 Ma|Of the Cleland Supersuite.|||Meta biotite granodiorite and minor pegmatitic granite; fine to medium grained; foliated.|11-NOV-16
33450|Kavir Granodiorite|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c. 3240 Ma|Of the Cleland Supersuite.|||Meta biotite granodiorite and minor pegmatitic granite; fine to medium grained; foliated.|02-MAY-14
33450|Kavir Granodiorite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Cleland Supersuite|||Meta biotite granodiorite and minor pegmatitic granite; fine to medium grained; foliated.|
33450|Kavir Granodiorite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|3240 Ma (isotopic)|Unit of Cleland Supersuite.|||Metamorphosed biotite granodiorite and minor pegmatitic granite; fine to medium grained; foliated|
33450|Kavir Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite, granite|
33450|Kavir Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|||Cleland Supersuite|||Metamoprhosed biotite granodiorite and minor pegmatitic granite; fine to medium grained; foliated.|
22076|Kazput Formation|23047|5|Briefly described|38|||Of the Turee Creek Group. Hamersley Province.  Underlain by Koolbye Formation.||||||10-FEB-09
22076|Kazput Formation|23280|6|Mentioned|p1089,Table1p1085|||||||||
22076|Kazput Formation|23890|4|Described|p16|Paleoproterozoic|Archean|Of Turee Creek Group. Geological Province: Pilbara Craton.||||||07-NOV-08
22076|Kazput Formation|24544|4|Described|p47 Fig.35|Paleoproterozoic|Paleoproterozoic|Conformably overlies Koolbye Formation. Unconformably overlain by Beasley River Quartzite. Of Turee Creek Group.  Geological Province: Ashburton Province.||||||07-NOV-08
22076|Kazput Formation|24607|5|Briefly described|p969 Fig. 2|||Of the Turee Creek Group.||||||
22076|Kazput Formation|43262|5|Briefly described|Map Legend||Proterozoic|of Turee Creek Group.||||||
22076|Kazput Formation|43290|3|Fully described|p8||Proterozoic|of Turee Creek Group.||||||
22076|Kazput Formation|60373|5|Briefly described|p145 Tb. 1|||Of Turee Creek Group. Underlain by Koolbye Formation.||||||18-SEP-15
22076|Kazput Formation|62129|3|Fully described|p12|Archaean|Archaean|Of Turee Creek Group. Overlies conformably Koolbye Formation, unconformably overlain by Beasley River Quartzite. Thickness: 1100m. Geological Province: Hamersley Basin.||||||18-SEP-15
22076|Kazput Formation|62130|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Turee Creek Group. Geological Province: Hamersley Basin, Pilbara Craton. Pelite, metasandstone, metaconglomerate, metadolerite, and banded iron-formation.||||||23-MAR-09
22076|Kazput Formation|66574|4|Described|p914 Fig.3|||Top of Turee Creek Group. Underlies Beasley River Quartzite, overlies Koolbye Formation. Lower is prograding shallow marine dolostone and siltstone to fluvial sandstone; upper is shallow marine sandstone and siltstone. McGrath Trough fill.||||||
22076|Kazput Formation|67130|5|Briefly described|p3 fig 2, p6, p24 fig 17, p31, p39|||Stromatolitic carbonate at least 360m thick.||Turee Creek Group||Overlies Koolbye Formation,|Carbonates with stromatolites, siltstone, sandstone, and conglomerate.|
22076|Kazput Formation|67183|6|Mentioned|p645 Tb.1|Archean|Archean|Present in the Southern Pilbara.||Turee Creek Group||||
22076|Kazput Formation|68035|5|Briefly described|p292, Fig 6|Paleoproterozoic|Paleoproterozoic|Turee Creek Basin.||||Overlies Koolbye Formation. Unconformably overlain by Beasley River Quartzite, Three Corners Conglomerate Member.|Carbonate, sandstone, siltstone.|
22076|Kazput Formation|68280|5|Briefly described|p5, p44, p51, p54, p55|Paleoproterozoic|Paleoproterozoic|||Turee Creek Group||Unconformably overlain by Cheela Springs Basalt, overlies Koolbye Formation|Fine grained sandstone, siltstone, jaspilitic chert and stromatolitic dolomite.|
22076|Kazput Formation|69003|5|Briefly described|p7-8|||Turee Creek Basin.||Turee Creek Group.||Unconformably overlies Koolbye Formation. Is overlain unconformably by Beasley River Quartzite.|Deltaic and shallow-marine sandstones, siltstones and dolostones.|
22076|Kazput Formation|69028|5|Briefly described|Map Legend|Siderian|Siderian|Turee Creek Basin. Mapped with Koolbye and Kungarra Formations as a single unit.|2445-2210 Ma|Of the Turee Creek Group.|||Mudstone, siltstone, sandstone, conglomerate, local stromatolitic dolomite and basalt; metamorphosed.|07-MAY-14
22076|Kazput Formation|69565|6|Mentioned|p133 Fig.1|||Hamersley Province.||Turee Creek Group.||Overlies Koolbye Formation. Is overlain by Beasley River Quartzite (Wyloo Group).||
22076|Kazput Formation|69754|6|Mentioned|p315, p317, p340|||Pilbara Craton.||Turee Creek Group||Overlies the Koolbye Formation.||
22076|Kazput Formation|70086|4|Described|p194-200,202-205,209|Paleoproterozoic|Paleoproterozoic|Geological province: Pilbara Craton. Of the Hamersley Basin. Thickness: ~750m. Lithology described are a composite description from localities in the study, and does not necessarily representative of Kazput Formation stratigraphy. Evidence of active syn-depositional extensional tectonism (mumerous cm to dm scale synsedimentary normal faults). Stromatolite domes are deposited stratigraphically after GOE. Large stromatolitic clasts and rip-ups are interpreted to be seismically-generated breccias (seismites) or the erosion of locally uplifted strata.||Unit of Turee Creek Group.||Overlain by Beasley River Quartzite/Wyloo Group.|Basal section of silty and carbonate-rich (stromatolitic) strata, grading upwards to sandy dolomite and into medium-bedded dolomitic sandstone (stromatolitic), becoming more calcareous and capped by massive gray dolomite.|
22076|Kazput Formation|70327|5|Briefly described|p4|||Thorne et al. (1995). Hamersley Province.||Turee Creek Group.||Is overlain unconformably by Beasley River Quartzite.||
22076|Kazput Formation|70795|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|West Australian Craton, Turee Creek Basin|2449-2208 Ma||||Pelite, metasandstone and metaconglomerate; minor recrystallized metadolomite and thin beds of metamorphosed banded iron formation.|
22076|Kazput Formation|71042|5|Briefly described|p66 fig 2|Paleoproterozoic|Paleoproterozoic|||Turee Creek Group||||
22076|Kazput Formation|71112|5|Briefly described|p69,73-74,76-77,80-81|||Geological province: Pilbara Craton. Carbonate platform.||||Underlain (locally unconformably) by Koolbye Formation.|Dolostones and siliciclastic mudrocks.|
22076|Kazput Formation|71550|4|Described|p35-38,40,42-45|Siderian|Siderian|Geological province: Of Hamersley Basin. Depositional environment: fluvial and shallow marine. U-Pb zircon analysis from a sandstone bar from this study yield maximum age of 2.34 Ga. Detrital provenance is likely from erosive products of underlyng Hamersley Province and Pilbara basement.||Unit of Turee Creek Group.||Uppermost unit of Turee Creek Group. Overlain by Beasley River Quartzite/Wyloo Group. Underlain by Koolbye Formation.|shales and stromatolitic marine carbonates.|03-SEP-19
22076|Kazput Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Turee Creek Basin.||Turee Creek Group|||Argillite, sandstone, and conglomerate; minor grey recrystallized dolomite and limestone, and thin beds of iron formation.|
22076|Kazput Formation|72570|5|Briefly described|p2|||||Turee Creek Group||Conformably overlies the Koolbye Formation.|Siliciclastic units and interbedded stromatolites and thinly bedded dolomite.|
22076|Kazput Formation|72712|3|Fully described|p1, p5, p14, p9, p21-25, p44.|Paleoproterozoic|Paleoproterozoic|Revised herein; originally defined by Thorne and Tyler (1996). See also Munder Formation. Estimated composite thickness of about 1000 m. Includes three diagnostic stromatolite assemblages that are useful for regional correlation (Allen, 2019). Incorporates the upper three original unnamed units of Trendall (1979). Age constraints on the MDA of the Kazput Formation come from two samples (Pi 15.41 and Pi 15.42) assigned by Caquineau et al. (2018). See also p26, p28, p29, p36 Fig.25, p43, p47.||Turee Creek Group|Includes Wonangara Member.|Conformably overlies Koolbye Formation and is unconformably overlain by Munder Formation.|Consists mainly of shallow-marine carbonate and fine grained siliciclastic rocks. Includes shales with intermittent dolomite limestone, marls. Also includes stromatolites and abundant hummocky bedding in the fine-grained siliciclastic lithologies.|14-JAN-21
22076|Kazput Formation|73538|5|Briefly described|p2 Fig. 1B, p3-4, App TbS1|||||Turee Creek Group||Underlain by Koolbye Formation. Overlain by Beasley River Quartzite (Wyloo Group).|Shales and stromatolitic marine carbonates.|
40192|Keene Basalt|61023|5|Briefly described|p16|||Mafic extrusive unit. Geological Province: Officer Basin.||||||11-APR-08
40192|Keene Basalt|61716|5|Briefly described|p642|Neoproterozoic|Neoproterozoic|Within the Kanpa Formation. Altered amygdaloidal basalt flow.  Thickness: 50m.||||||19-MAY-06
40192|Keene Basalt|62453|4|Described|p5 Fig. 3, 33, 70|Cryogenian|Cryogenian|Of the Buldya Group. Geological Province: Officer Basin. Intercalated with Kanpa Formation. ||||||
40192|Keene Basalt|63022|4|Described|p1013, p1016 Fig. 2, p1017|Neoproterozoic|Neoproterozoic|Tholeiitic basalt flow intersected in GSWA drillhole Lancer 1, in shallow marine Kanpa Formation (Haines et al, 2004) - extruded between the two lowest two dolostone units. Geol.Prov: Officer Basin. Thickness: 49m. Fine-to coarse-gr, locally amygdaloidal.||||||10-AUG-07
40192|Keene Basalt|64103|6|Mentioned|p400 Fig. 3|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||07-FEB-11
40192|Keene Basalt|65363|2|Defined|p1, p6 Fig.5, p8, p37.|Neoproterozoic|Neoproterozoic|New name, after Lake Keene, 10 km west of the drillhole subject of this report. Type section is the interval 527.4 to 576.2 m in Lancer 1. Regarded as a separate unit rather than part of Kanpa Formation or Buldya Group. Four or five flows over wet dolostone sediment. The second record of extrusive igneous rocks within the Neoproterozoic succession of Western Australia. Could correlate with, but is not comagmatic with, Cadlareena Volcanics of northeastern Officer Basin in South Australia as well as the Boucaut Volcanics in the Adelaide Rift Complex.|c.760 ma.||||Dark grey to greenish basalt, fine-grained, coarse-grained and massive in middle of each flow, locally amygdaloidal and brecciated; veins and amygdales filled with calcite, red chert or chlorite; erosional topmost surface; no interbedded sediments.|03-SEP-14
40192|Keene Basalt|65364|5|Briefly described|p81|||Officer Basin.||||Overlain unconformably by Kanpa Formation, underlain by Hussar Formation.|Dark, fine- to coarse-grained basalt, locally amygdaloidal; erosional upper surface.|16-MAR-12
40192|Keene Basalt|65365|5|Briefly described|p8 Fig.3|||Of the Buldya Group.||||||19-MAR-12
40192|Keene Basalt|65366|5|Briefly described|p19|||||||||
40192|Keene Basalt|65368|6|Mentioned|p12, p14 Fig 1, p16 Fig. 2, p17 Fig. 3-4|Neoproterozoic|Neoproterozoic|||||||
40192|Keene Basalt|65369|4|Described|p29-34 Tb. 1, 35, 36|||Officer Basin. Tholeiitic basalt of intraplate continental origin. Possibly correlative with the Gairdner Dyke Swarm and Mingary dykes.|||||5 basalt flows; variably vesicular, locally lithic rich, celadonite and iddingsite common.|19-APR-13
40192|Keene Basalt|65371|6|Mentioned|p54 Fig. 1|||Within Kanpa Formation. Extrusive flows.||||||
40192|Keene Basalt|67454|4|Described|p563 Fig.2, pp564-568, p570.|Neoproterozoic|Neoproterozoic|Officer Basin. 49 m thick. Palaeomagnetic results from the Lancer 1 drillhole are detailed and discussed.|c.750 Ma.|Unit in Kanpa Formation.|||Four or five flows: tops and bases are fine-grained and amygdaloidal; coarse-grained massive basalt flow centres.|
40192|Keene Basalt|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|Officer Basin.||Buldya Group.||||
40192|Keene Basalt|69091|6|Mentioned|p176|||Intersected in GSWA Lancer 1 drill hole.||||||26-SEP-14
40192|Keene Basalt|71001|6|Mentioned|p22|Tonian|Tonian|Officer Basin. 49m thick.||Kanpa Formation.|||Subaerially extruded basalt.|
40192|Keene Basalt|72601|6|Mentioned|p6|Tonian|Tonian|Volcanic unit within the Kanpa Formation. Geochronologic constraint by (Zi et al., 2017).|ca 752 Ma 40Ar/39Ar|||Equivalent to or intrudes Kanpa Formation.||
33451|Keep It Dark Monzogranite|23416|5|Briefly described|Map Legend|Archean|Archean|In the Pilbara Craton.||||||07-NOV-08
33451|Keep It Dark Monzogranite|23755|4|Described|p47|Archean|Archean|Age: c.2.94 Ga.||||||07-NOV-08
33451|Keep It Dark Monzogranite|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Age: 2936+/-5Ma (Van Kranendonk, 2000).  Geological Province: Pilbara Craton.||||||07-NOV-08
33451|Keep It Dark Monzogranite|24110|5|Briefly described|Plate 1|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
33451|Keep It Dark Monzogranite|63441|5|Briefly described|p11 Tb. 2|Archean|Archean|Of Sisters Supersuite. Age: 2936+/-5Ma. Geological province: Pilbara Craton.||||||07-FEB-11
33451|Keep It Dark Monzogranite|64580|4|Described|map legend||Mesoarchean|Of Sisters Supersuite. Monzogranite; undeformed to foliated; medium-grained, equigranular to weakly porphyritic; weakly metamorphosed.||||||15-DEC-08
33451|Keep It Dark Monzogranite|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Unit in Sisters Supersuite. c.2936 Ma. Monzogranite; undeformed to foliated; medium-grained, equigranular to weakly porphyritic; weakly metamorphosed.||||||
33451|Keep It Dark Monzogranite|69015|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton. Includes 1 unnamed sub-unit. Also appears as misspelt Keep it Dark Monzogranite.|c.2936 Ma|Of the Sisters Supersuite.|||Equigranular monzogranite, locally weakly porphyritic, metamorphosed; porphyritic monzogranite, locally equigranular, metamorphosed.|02-MAY-14
33451|Keep It Dark Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Sisters Supersuite|||Porphyritic monzogranite; locally equigranular; metamorphosed|
33451|Keep It Dark Monzogranite|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.||Unit of Sisters Supersuite.|||Hornblende granite; massive; iron oxide and hornblende replaced by chlorite|
33451|Keep It Dark Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; North Pilbara Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.|2936 Ma (isotopic)|Unit of Sisters Supersuite.|||Porphyritic and equigranular monzogranite; locally equigranular; metamorphosed|
33451|Keep It Dark Monzogranite|71137|6|Mentioned|p3|Archean|Archean|Pilbara.|2936 +/- 5 Ma (SHRIMP: van Kranendonk, 2000).|||Intrudes Lalla Rookh Formation.||
33451|Keep It Dark Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
33451|Keep It Dark Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Sisters Supersuite|||Porphyritic monzogranite; locally equigranular; metamorphosed.|
69691|Kelly Group|61111|6|Mentioned|p98|||Includes the Strelley Pool Chert? Volcanic rocks of the rest of the Kelly Group conformably overlie the Strelley Pool Chert||||||
69691|Kelly Group|61253|5|Briefly described|p51, p50 Fig. 1, p52 Fig. 2, p58|Archean|Archean|Formerly Kelly Subgroup (of Warrawoona Gp). Still includes subgroup components: Strelley Pool Chert, Euro Basalt, Wyman Fm and Charteris Basalt. Now of the Pilbara Supergroup.Unconformable beneath Nullagine Gp. Age: 3.35-3.30Ga. Geol.Prov: Pilbara Craton.||||||07-NOV-08
69691|Kelly Group|61264|5|Briefly described|p64 Fig. 2|||Of the Pilbara Supergroup. Geological Province: East Pilbara Granite-Greenstone Terrane/Pilbara Craton.||||||
69691|Kelly Group|62979|5|Briefly described|p211, p213|||Includes Strelley Pool Chert and Euro Basalt. Lower parts extensively silicified. Overlies the Warrawoona Group. Together with Kelly Group forms North Pole Dome. Geological Province: Pilbara Craton.||||||07-FEB-11
69691|Kelly Group|63142|5|Briefly described|p487|Archean|Archean|Age: ca 3.35-3.31Ga. Overlies the Warrawoona Group.||||||07-NOV-08
69691|Kelly Group|63245|5|Briefly described|p5|Archean|Archean|Of the Pilbara Supergroup. Age: ca.3.43-3.32Ga. Geological Province: Pilbara Craton.||||||07-NOV-08
69691|Kelly Group|63367|6|Mentioned|p244-245. |Paleoarchean|Paleoarchean|Pilbara Craton.|||Includes Strelley Pool Chert.|||
69691|Kelly Group|63417|5|Briefly described|Map legend|Archean|Archean|Of the Pilbara Supergroup.  Includes Strelley Pool Chert, Euro Basalt, Wyman Formation and Charteris Basalt.  Includes rocks with ages: c.3350Ma and 3325-3315Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
69691|Kelly Group|63420|5|Briefly described|Map legend|Archean|Archean|Of the Pilbara Supergroup. Includes Strelley Pool Chert, Euro Basalt and Wyman Formation. Age: c3350-3335Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
69691|Kelly Group|63441|3|Fully described|p4 Tb. 1, p20|Archean|Archean|Of the Pilbara Supergroup. Supersedes Kelly Subgroup. Includes Strelley Pool Chert, Euro Basalt, Wyman Fm. and Charteris Basalt. Age: 3350-3300Ma. Max. thickness: ~7000m. Geological Province: Pilbara Craton/east Pilbara Terrane.||||||07-FEB-11
69691|Kelly Group|63538|4|Described|p2 Fig. 1, p3 Fig. 2, p5, p9-10, p11|Archean|Archean|Of Pilbara Supergroup. Includes Wyman Formation, Euro Basalt and Strelley Pool Chert. Age: 3350-3300 Ma. Geological Province: Pilbara Craton.||||||17-APR-13
69691|Kelly Group|63649|5|Briefly described|p201|Archean|Archean|Of the Pilbara Supergroup. Includes Strelley Pool Chert, Euro Basalt and Wyman Formation. Unconformably overlies Warrawoona Group. Age: 3.43 - 3.31Ga. Geological Province: Pilbara Craton.||||||07-FEB-11
69691|Kelly Group|63854|6|Mentioned|p229 Fig.2 |||||Unit in Pilbara Supergroup.|Includes the Wyman Formation, Euro Basalt and the Strelley Pool Chert.|||
69691|Kelly Group|64405|5|Briefly described|p1, p21|Archean|Archean|Of the Pilbara Supergroup. Contains the Euro Basalt. Geological province: East Pilbara Terrane. Discussion in favour of and against placing Strelley Pool Chert within this group is presented (p20-21).||||||07-FEB-11
69691|Kelly Group|64621|5|Briefly described|Map legend|Archean|Archean|Of the Pilbara Supergroup. Includes Euro Basalt and Wyman Formation. Comprehensive lithological details included.||||||07-NOV-08
69691|Kelly Group|64632|5|Briefly described|p201 Fig.1|Paleoarchean|Paleoarchean|East Pilbara terrane. Up to 8km thick. Age given as 3.35-3.315 Ga on p202.Age generalised in Fig 1?|3350-3315 Ma|Of the Pilbara Supergroup.||Unconformably underlain by the Warrawoona Group. Overlain by Sulphur Springs Group.|Tholeiitic basalt, basaltic komatiite, and komatiite, capped by rhyolite.|
69691|Kelly Group|64654|5|Briefly described|Map Legend|Archaean|Archaean|Of Pilbara Supergroup. Includes Euro Basalt. Age: 3350-3335Ma. Geological Province: Pilbara Craton.||||||17-NOV-08
69691|Kelly Group|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Pilbara Supergroup. Includes Euro Basalt. Geological Province: Pilbara Craton.||||||
69691|Kelly Group|65724|5|Briefly described|map legend|Paleoarchaean|Paleoarchaean|Of Pilbara Supergroup. Geol. Prov: East Pilbara Granite-Greenstone Terrane.||||||
69691|Kelly Group|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Post-dates the Warrawoona event c.3410 Ma.||Of Pilbara Supergroup. |Includes Charteris Basalt, Wyman Formation, Euro Basalt and Strelley Pool Chert.|||
69691|Kelly Group|65825|4|Described|p5, p32.|Archean|Archean|Formerly the Kelly Subgroup. In the 2004 redefinition of the Pilbara Supergroup by Van Kranendonk et al., this unit includes all rocks assigned to the Warrawoona Group.||Unit in the redefined Pilbara Supergroup of Van Kranendonk et al. (2004).|Includes Wyman Formation and Euro Basalt.|||
69691|Kelly Group|65827|3|Fully described|p1, p6 Tb.1, p8, p9 Fig 3, p15, p20-22 |Paleoarchean|Paleoarchean|3350-3315 Ma. Of Pilbara Supergroup; formerly Kelly Subgroup (of Warrawoona Group). Unconformably overlies Warrawoona Group; unconformably underlies Gorge Creek Group. Includes Charteris Basalt, Wyman Formation, Strelley Pool Chert, Euro Basalt.||||||
69691|Kelly Group|65829|5|Briefly described|p1, p7 Fig.3, p13. |Paleoarchean|Paleoarchean|Defined by Van Kranendonk et al. (2004b).|3420 - 3315 Ma (Van Kranendonk et al. 2006).||Comprises basal Strelley Pool Chert, Euro Basalt, Wyman Formation and Charteris Basalt.|||18-DEC-12
69691|Kelly Group|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit of Pilbara Supergroup. Comprises Euro Basalt, Wyman Formation, and Charteris Basalt.||||||
69691|Kelly Group|66118|4|Described|p146 Fig.1, p147-149, p157-158|||Pilbara Craton. East Pilbara Terrane. Shown as Warrowoona, Kelly, and Sulphur Springs Group in Fig.2.|3350-3300 Ma; 3350-3325 Ma|Pilbara Supergroup|Strelley Pool Formation|Is unconformably overlain by Sulphur Springs Group. Unconformably overlies Warrawoona Group.|Plume-derived succession of ultramafic through rhyolitic volcanic rocks. Komatiitic metabasalts commonly pillowed, greenschist facies.|
69691|Kelly Group|66122|6|Mentioned|p74|Archean|Archean||3.35 - 3.31 Ga.|Pilbara Supergroup.||||
69691|Kelly Group|66217|3|Fully described|p1, p5, p6, p8, p10, p14, pp29-31, p36.|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Of Van Kranendonk et al. (2006a, 2007); elevated from Subgroup status on the basis of a regional unconformity beneath the Strelley Pool Formation. Up to 9000 m thick. |c.3350-3315 Ma.|Unit in Pilbara Supergroup.|Includes Euro Basalt and Wyman Formation.|Conformably overlies Strelley Pool Formation. Unconformably overlies Warrawoona Group. Is unconformably overlain by Sulphur Springs Group.|Thick volcanic succession of interbedded basalt, komatiitic basalt, and komatiite (Euro Basalt); and a major unit of high-K rhyolite (Wyman Formation).|
69691|Kelly Group|66664|4|Described|p3, p6, p7, p8.|||East Pilbara Terrane||Part of Pilbara Supergroup.|Includes Euro Basalt.||Tholeiitic pillow basalt; dolerite and gabbros; basaltic komatiite as pillows, flows and intrusions.|
69691|Kelly Group|66685|6|Mentioned|p234|Early Archean|Early Archean|REE + Y analysis by Van Kranendonk et al.(2003) suggested an anoxic marine origin for stromatolitic dolomites.||||||
69691|Kelly Group|66745|4|Described|pp50-59.|Paleoarchean|Paleoarchean|Mantle plume event producing volcanic formations above a thin sedimentary unit, the Strelley Pool Formation, which had been included as a basal unit within this Group but is now removed.|3350-3315 Ma.|Unit in Pilbara Supergroup.|Includes basal Euro Basalt, Wyman Formation and Charteris Basalt.|Overlies Strelley Pool Formation or, where that unit is absent, the Warrawoona Group. Is unconformably overlain by Budjan Creek Formation.||
69691|Kelly Group|66887|5|Briefly described|p21 Fig.11|||Pilbara Craton.|~3350-~3330 Ma estimated from Fig.11.|||||
69691|Kelly Group|67130|6|Mentioned|p16, p17, p62, p77|||Misspellt as Kelley Group (p77)||Pilbara Supergroup|Includes Euro Basalt|Overlies Warrawoona Group, overlain by Sulphur Springs Group||
69691|Kelly Group|67197|5|Briefly described|p1-5, p9, p13-14, p19, p22, p29, p33-34|Paleoarchean|Paleoarchean|See also p36. Pilbara Craton.|3350-3315 Ma.|Pilbara Supergroup.|Euro, Charteris Basalts; Wyman Formation.|Unconformably overlies Strelley Pool Formation. Is overlain by Sulphur Springs Group.||
69691|Kelly Group|67201|4|Described|p7 Fig.4, p10-12|||In northern Pilbara Craton, East Pilbara Terrane. Thermal event resposible for Kelly Group and Emu Pool Supersuite ceased at c. 3290 Ma.|3350-3315 Ma|Pilbara Supergroup|Charteris Basalt, Wyman Formation, Euro Basalt|Disconformably overlies Strelley Pool Formation. Is erosionally overlain (unconformity) by Sulphur Springs Group.||
69691|Kelly Group|67269|5|Briefly described|p2-3, p6-7 Figs.3-4, p14|Paleoarchean|Paleoarchean|Van Kranendonk et al. (2004) renamed the Strelley Pool Chert as the Strelley Pool Formation, and moved it from Warrawoona Group into this Group.|3350-3315 Ma.|Pilbara Supergroup.|Euro, Charteris Basalts; Wyman Formation.|Overlies Strelley Pool Formation. Is overlain by Sulphur Springs Group.||
69691|Kelly Group|67270|5|Briefly described|p2-4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Pilbara Supergroup.|Euro, Charteris Basalts; Wyman Formation.|Unconformably overlies Strelley Pool Formation. Is overlain unconformably by Sulphur Springs Group.||
69691|Kelly Group|67668|6|Mentioned|Fig. 2; p. 154, 157; Tb.1. ||Paleoarchean|East Pilbara Terrane, Pilbara Craton.|3350 - c.3270 Ma.|Pilbara Supergroup|Euro Basalt, Wyman Formation, Charteris Basalt.|Underlies the Sulphur Springs Group, overlies the Strelley Pool Formation.|Dominantly volcanic.|
69691|Kelly Group|68035|4|Described|p287,  p286 Fig 3, p288 Fig 4|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Erosional unconformity of ~60 million years to overlying Sulphur Springs Group.|Max age 3350 Ma, Min age 3315 Ma|Of Pilbara Supergroup.|Includes Euro Basalt, Wyman Formation, Charteris Basalt.|Unconformably overlies Warrawoona Group.Overlies Strelley Pool Formation. Unconformably overlain by Sulphur Springs Group|Basalt, felsic volcanics, lesser  komatiitic basalt, komatiite, chert.|
69691|Kelly Group|68280|6|Mentioned|p1, p4||||||Includes Euro Basalt, Wyman Formation, Charteris Basalt|||
69691|Kelly Group|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Pilbara Supergroup.|Includes Wyman Formation, Euro Basalt.|||23-SEP-13
69691|Kelly Group|68282|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|3426-3255 Ma|Of the Pilbara Supergroup|Includes Euro Basalt.|||
69691|Kelly Group|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Pilbara Supergroup.|Includes Wyman Formation, Euro Basalt.|||19-JUN-14
69691|Kelly Group|68284|5|Briefly described|p4, 6-7, 9|Paleoarchean|Paleoarchean|Kelly greenstone belt, East Pilbara Terrane.|3350-c.3300 Ma.|Pilbara Supergroup.|Euro, Charteris Basalts; Wyman Formation.|Overlies Warrawoona Group. Is unconformably overlain locally by Sulphur Springs or Soanesville Group. Is intruded by Dalton Suite.|Komatiitic basalt; pillow basalt; layered, white, grey and blue-black chert.|
69691|Kelly Group|69012|5|Briefly described|Map Legend|Archean|Archean|East Pilbara Terrane.||Of the Pilbara Supergroup.|Includes the Wyman Formation and Euro Basalt.|||
69691|Kelly Group|69013|6|Mentioned|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Of the Pilbara Supergroup.|Includes the Euro Basalt.|||30-APR-14
69691|Kelly Group|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Pilbara Supergroup.|Includes Euro Basalt.|||
69691|Kelly Group|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Pilbara Supergroup|Includes Euro Basalt|||
69691|Kelly Group|69185|5|Briefly described|500k_geologyp08_lut.csv|||Geological Province: Pilbara Craton.||Unit of Pilbara Supergroup.|Includes Wyman Formation.|||
69691|Kelly Group|69301|4|Described|p5 Fig.3, p9 Tb.1, p11, p20-21|||Pilbara Craton. East Pilbara Terrane.|3350-3320 Ma from unit ages|Pilbara Supergroup|Charteris Basalt, Wyman Formation, Euro Basalt|Disconformably overlies Strelley Pool Formation. Unconformably overlies Warrawoona Group (regionally). Is unconformably overlain by Sulphur Springs Group.||
69691|Kelly Group|69566|5|Briefly described|p236-237, 241|||East Pilbara Granite-Greenstone Terrane. <9km thick.|3335-3312 Ma.||Euro, Charteris Basalts; Wyman Formation.|Unconformably overlies Warrawoona Group. Is overlain by George Creek Group.||
69691|Kelly Group|69590|5|Briefly described|GEOL_LUT_CSV files|||Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 250k_interpgeol_lut.csv.||Unit of Pilbara Supergroup.|Includes Charteris Basalt, Euro Basalt, Wyman Formation.|||
69691|Kelly Group|69616|6|Mentioned|p161|Archean|Archean|||||Is overlain unconformably by Sulphur Springs Group.||
69691|Kelly Group|69740|5|Briefly described|p651, 663, 676|Paleoarchean|Paleoarchean|Suprasubduction zone; forearc plume magmatism.|3.35-3.29 Ga.|Pilbara Supergroup.|||Mainly basaltic pillow lava, minor felsic and ultramafic lavas, chert layers.|
69691|Kelly Group|70022|5|Briefly described|p113-116|||Warralong Greenstone Belt, East Pilbara Terrane.|3350-3300 Ma.|Pilbara Supergroup.|Wyman Formation; Euro, Charteris Basalts.|Overlies Strelley Pool Formation. Is overlain unconformably by Sulphur Springs Group.||
69691|Kelly Group|70507|5|Briefly described|p431|Archean|Archean|Geological province: Pilbara Craton.|||Includes Euro Basalt and Strelley Pool Formation.|||
69691|Kelly Group|70729|6|Mentioned|p163-164|||Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Pilbara Supergroup.||||
69691|Kelly Group|70733|6|Mentioned|p105|||Eastern Pilbara Craton.||Pilbara Supergroup.||||
69691|Kelly Group|70775|5|Briefly described|p12, p100|Paleoarchean|Paleoarchean|East Pilbara.|c. 3320-3350 Ma|Pilbara Supergroup|Includes the Strelley Pool Formation, Euro Basalt, Wyman Formation and the Charteris Basalt.|Disconformably overlies the Strelley Pool Formation. Unconformably overlain by the Sulphur Springs Group.||
69691|Kelly Group|70826|6|Mentioned|p8|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Pilbara Supergroup||Unconformably overlies the Warrawoona Group.||12-MAY-20
69691|Kelly Group|70884|5|Briefly described|p123,135-137|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Thickness: 7.5km thick.||Unit of Pilbara Supergroup.|Includes Charteris Basalt. Wyman Formation and Euro Basalt.|Overlain unconformably by Sulphur Springs Group/Leilira Formation. Underlainunconformably by Strelley Pool Formation.||
69691|Kelly Group|71041|6|Mentioned|p44|||||||||
69691|Kelly Group|71137|6|Mentioned|p2, 4-5, 12|Archean|Archean|||||Is overlain unconformably by Farrel Quartzite (Gorge Creek Group).||
69691|Kelly Group|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||volcaniclastic rock, sandstone, siltstone, shale, amphibolite, mafic schist, leucogabbro, dolerite, ultramafic schist, ultramafic rock|
69691|Kelly Group|71270|5|Briefly described|1m_geologyl12_lut.csv|||Geological province: Yilgarn Craton, West Australian Craton. ||Unit of Pilbara Supergroup.|||Ultramafic rock|
69691|Kelly Group|71487|5|Briefly described|p127-128|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|3350-3315 Ma|Unit of Pilbara Supergroup.|Includes Euro Basalt.|Overlain by Sulphur Springs Group. Underlain by Strelley Pool Formation.||
69691|Kelly Group|72034|6|Mentioned|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Charteris Basalt, Wyman Formation, Euro Basalt.|||
69691|Kelly Group|72064|5|Briefly described|p65-66|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|c. 3350-3310 Ma|Unit of Pilbara Supergroup.|Includes Charteris Basalt, Wyman Formation and Euro Basalt.|Overlain unconformably by Sulphur Springs Group/Leilira Formation. Underlain by Strelley Pool Formation.||
69691|Kelly Group|72251|5|Briefly described|p52-54|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|3350-3300 Ma|Unit of Pilbara Supergroup.|Includes Charteris Basalt, Wyman Formation and Euro Basalt.|Overlain unconformably by Suphur Springs Group.||11-FEB-20
69691|Kelly Group|72668|5|Briefly described|p3-5, p7, p9-10, p18, p24, p26|||East Pilbara Terrane. Geochemistry is discussed.|c 3350-3300 Ma|Pilbara Supergroup|Includes the Charteris Basalt, Wyman Formation, Euro Basalt and the Strelley Pool Chert.|Unconformably overlies the Coonterunah Subgroup and the Warrawoona Group.||13-JAN-22
69691|Kelly Group|73160|6|Mentioned|p2 Fig.1|||Pilbara Craton.|||Strelly Pool Formation, Euro Basalt.|Overlies Warrawoona Group. Unconformably underlies De Grey Supergroup.||
69691|Kelly Group|73598|5|Briefly described|p1207, 1209, 1212-1213|Paleoarchean|Paleoarchean|East Pilbara Terrane.|3350-3320 Ma.|Pilbara Supergroup.|Euro, Charteris Basalts; Wyman Formation.|Overlies Strelley Pool Formation. Is overlain unconformably by Sulphur Springs Group.|Includes dolerite dykes.|
35485|Ken's Bore Granite|23209|6|Mentioned|p16|||||||||
74628|Kennedys Cottage Limestone|64449|2|Defined|p75, p76, p79 Tb. 5, p107, p111|Holocene|Holocene|Overlies Willie Creek Calcarenite, underlies Horsewater Soak Calcarenite. Age: 5500+/-160 yrs BP and 5590+/-240 yrs BP. Thickness: 2m. Cross-laminated  shelly calcarenite and calcarenite. See p107 and 111.||||||07-FEB-11
74628|Kennedys Cottage Limestone|73213|5|Briefly described|958 Fig.3(b), 967-968|||Mid-Holocene.||||Overlies Willie Creek Calcarenite. Is overlain by Horsewater Soak Calcarenite.|Limestone, originally beach deposits.|19-JAN-23
39505|Kennell Granodiorite|63417|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite.  Age: c.3315Ma. Geol.Province: Pilbara Craton. Biotite-hornblende granodiorite, locally includes monzogranite and tonalite; medium-grained; seriate, weakly foliated; small mafic xenoliths and schleren locally common; metamorphosed.||||||07-NOV-08
39505|Kennell Granodiorite|63441|5|Briefly described|p8 Tb. 2|Archean|Archean|Of Emu Pool Supersuite. Replaces Yandicoogina Suite. Age: 3315+/-2Ma. Geological province: Pilbara Craton.||||||07-FEB-11
39505|Kennell Granodiorite|64621|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite. Age: 3315Ma. Biotite-hornblende granodiorite, local monzogranite and tonalite, foliated; local mafic xenoliths and schlieren; metamorphosed.||||||07-NOV-08
39505|Kennell Granodiorite|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.|c.3315 Ma (Nelson 2002).|Of Mount Edgar Granitoid Complex.|||Biotite-hornblende granodiorite, monzogranite and tonalite; medium- to coarse-grained, weakly to moderately foliated; small mafic xenoliths and schlieren; granitoid rock with mafic and ultramafic xenoliths and rafts.|
39505|Kennell Granodiorite|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c.3315 Ma.|Of Emu Pool Supersuite.|||Biotite-hornblende granodiorite; local monzogranite and tonalite; medium-grained, weakly foliated; local mafic xenoliths and schlieren; granitic rock with mafic and ultramafic xenoliths; metamorphosed.|
39505|Kennell Granodiorite|65827|2|Defined|p6 Tb.2, p14 Tb.4, p16, p24, p27, p58|Paleoarchean|Paleoarchean|New name; after Kennell Well. Irregular intrusion, up to 37 x 10 km. Corresponds in part to Yandicoogina Suite.|3315 +/- 2 Ma (SHRIMP U-Pb zircon; Nelson 2002).|Of Emu Pool Supersuite.||Intruded by Bishop Creek Monzogranite; intrudes Duffer Formation, Apex Basalt, Underwood and Fig Tree Gneisses, Davitt Syenogranite, Joorina and Chessman Granodiorites.|Grey, biotite-hornblende tonalite, granodiorite and minor monzogranite; many xenoliths.|21-MAY-14
39505|Kennell Granodiorite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Emu Pool Supersuite. 3315-3312 Ma. Biotite-hornblende granodiorite; local monzogranite and tonalite; foliated; local mafic xenoliths and schlieren; metamorphosed.||||||
39505|Kennell Granodiorite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Intruded by unnamed porphyry||Emu Pool Supersuite|||Biotite hornblende granodiorite; local monzogranite and tonalite; foliated; local mafic and ultramafic xenoliths and schlieren; metamorphosed.|
39505|Kennell Granodiorite|69566|6|Mentioned|p236|||Mount Edgar Granitoid Complex, East Pilbara Granite-Greenstone Terrane.||Emu Pool Supersuite.||||
39505|Kennell Granodiorite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3315-3312 Ma (isotopic)|Unit of Emu Pool Supersuite.||Intrudes into Fig Tree Gneiss.|Biotite-hornblende granodiorite; local monzogranite and tonalite; foliated; local mafic xenoliths and schlieren; metamorphosed|
39505|Kennell Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite, monzogranite, tonalite|
39505|Kennell Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||Max age 3315+/-5 Ma, min 3312+/-4 Ma.|Emu Pool Supersuite|||Biotite-hornblende granodiorite; local monzogranite and tonalite; foliated; local mafic xenoliths and schlieren; metamorphosed.|
79017|Kents Bore Basalt|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2682 - 2671 Ma (inferred).|Gindalbie Group|||Basalt; aphyric and feldspar-phyric; metamorphosed. Plagioclase phyric basalt; metamorphosed.|
79017|Kents Bore Basalt|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2682-2676 Ma (inferred)|Unit of Gindalbie Group.|||Basalt; aphyric and feldspar-phyric, plagioclase-phyric; metamorphosed.|
30802|Kerba Granite|23485|5|Briefly described|p29|Paleoproterozoic|Paleoproterozoic|on MOORARIE 1:100 000 sheet.  Age: 1808+/-6Ma (SHRIMP U-Pb zircon)||||||07-NOV-08
30802|Kerba Granite|23592|4|Described|p13|Paleoproterozoic|Paleoproterozoic|Age: 1808+/-6 Ma. Of Moorarie Supersuite.||||||07-NOV-08
30802|Kerba Granite|44927|5|Briefly described|Map Legend||Paleoproterozoic|1808 +/- 6 Ma||||||07-NOV-08
30802|Kerba Granite|50221|5|Briefly described|p296 Fig.1, p303-4|||Biotite monzogranite intruding the Yarlarweelor Gneiss Complex. Age: 1808+/-6 ma.||||||
30802|Kerba Granite|65896|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Moorarie Supersuite. Even-textured, medium-grained, biotite monzogranite; locally foliated. c. 1808 Ma.||||||
30802|Kerba Granite|66299|4|Described|p148, p200.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. A large, thick granite sheet that outcrops as tors and pavements.|1808 +/- 6 Ma.|Unit in Moorarie Supersuite.||Intrudes Yarlarweelor Gneiss Complex. Is in faulted contact with Narracoota Formation.|Equigranular medium-grained biotite monzogranite; mainly massive, locally foliated to mylonitic; locally contains abundant inclusions of Archean granitic gneiss.|
30802|Kerba Granite|70804|5|Briefly described|p27|Palaeoproterozoic|Palaeoproterozoic|In contact with the Narracoota Formation, however; the nature of the contact is not provided.||||||
30802|Kerba Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
30802|Kerba Granite|71269|6|Mentioned|1m_geologyp12_lut.csv||||||||Equigranular locally foliated biotite monzogranite|
30802|Kerba Granite|71484|6|Mentioned|p125|||Geological province:Of Padbury Basin [?].||Unit of Mooranie Supersuite.|||Medium to even-textured biotite monzogranite, locally porphyritic.|30-AUG-19
30802|Kerba Granite|73214|5|Briefly described|p976|||Southern Capricorn Orogen.|1808 +/- 6 Ma (GSWA 142849).|Yarlarweelor Gneiss Complex||||
80031|Kerba Monzogranite|67888|6|Mentioned|p49|||GSWA reference material for geochemical analyses.||||||20-SEP-17
80031|Kerba Monzogranite|72251|6|Mentioned|p56|||||||||
80031|Kerba Monzogranite|73598|6|Mentioned|p1210|||Used as a geochemical reference.||||||
80609|Kestrel Cavern Gabbro|73084|4|Described|p: 15, 23-24, 27, 69, 71-72, 79...|Stenian|Stenian|Madura Province and[?] Coompana Province. Undeformed. Includes xenoliths of the Narilya Bore Basalt, although a genetic relationship is unlikely based on significantly different geochemical signatures. Quartz monzogabbro has cumulate texture. Report includes lithologic/petrographic description, whole-rock geochemistry, geochronology, Sm-Nd. [Also written as Kestrel Cavern Monzogabbro on p84 and Kestrel Cavern monzogabbro on p96 and p98]. Also p: 81-92, 96-98, 122-127, p133-134, p141.|1143 +/- 5 Ma, 1144 +/- 7 Ma|Moodini Supersuite||Intrudes Narilya Bore Basalt.|Medium- to coarse-grained (average 3-10 mm) quartz/ferro-monzogabbro, which grades to a very coarse-grained (average 10-15 mm), plagioclase-rich pegmatitic leucogabbro.|
29876|Kevins Dam Monzogranite|22547|6|Mentioned|p19|||||||||
29876|Kevins Dam Monzogranite|23751|4|Described|p17|Proterozoic|Proterozoic|Of Kevins Dam suite.||||||
29876|Kevins Dam Monzogranite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs Supersuite. Age: 1825Ma. Geological province: Kimberley Province.||||||07-FEB-11
29876|Kevins Dam Monzogranite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  In the Bow River batholith.  Age: 1835-1805Ma.||||||07-NOV-08
29876|Kevins Dam Monzogranite|43855|5|Briefly described|Map Legend||Proterozoic|||||||
29876|Kevins Dam Monzogranite|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|of Sally Downs supersuite.||||||
29876|Kevins Dam Monzogranite|44230|5|Briefly described|Map Legend||Proterozoic|||||||
29876|Kevins Dam Monzogranite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
29876|Kevins Dam Monzogranite|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Kevins Dam Suite (Sally Downs Supersuite). Used interchangeably with Kevins Dam Granite.||||||07-NOV-08
29876|Kevins Dam Monzogranite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Kevins Dam Suite|||Medium-grained, equigranular or weakly porphyritic biotite monzogranite.|31-JUL-15
29876|Kevins Dam Monzogranite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Kevins Dam Suite|||Medium grained equigranular to weakly porphyritic biotite monzogranite.|
29876|Kevins Dam Monzogranite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2.|1827-1808 Ma (Inferred)|Unit of Kevins Dam Suite.|||Medium-grained, equigranular or weakly porphyritic biotite monzogranite|
29876|Kevins Dam Monzogranite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1808-1827 Ma|Kevins Dam Suite|||Medium-grained, equigranular or weakly porphyritic biotite monzogranite|
29876|Kevins Dam Monzogranite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1827-1808 Ma (inferred)|Unit of Kevins Dam Suite.|||Medium-grained, equigranular or weakly porphyritic biotite monzogranite|
29876|Kevins Dam Monzogranite|72437|5|Briefly described|p87, p106|||Lamboo Complex. Whole-rock analyses are provided.||Kevins Dam Suite|||Biotite monzogranite.|
31898|Kevins Dam Suite|50437|6|Mentioned|p4.1|||Of the Sally Downs Supersuite. Geological Province: Kimberley Region.||||||
31898|Kevins Dam Suite|65359|5|Briefly described|p23, p28 Fig.28   |||East Kimberley region. High REE abundances. Contains biotite monzogranite.||||||
31898|Kevins Dam Suite|69099|5|Briefly described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.|||Includes Mount Christine and Shepherds Bore Granites; Dillinger, Kevins Dam, Koondooloo, Magotty Springs, Wesley Yard and Loadstone Monzogranites; Violet Valley Tonalite.||Granites, granodiorites, monzogranites, tonalites.|31-JUL-15
31898|Kevins Dam Suite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Also includes Magotty Springs Monzogranite,Shepherds Bore Granite, Violet Valley Tonalite, Wesley Yard Monzogranite, Loadstone Monzogranite.||Sally Downs Supersuite|Includes Mount Christine Granite, Dillinger Monzogranite, Kevins Dam Monzogranite, Koondooloo Monzogranite|||
31898|Kevins Dam Suite|69634|5|Briefly described|100k_interpgeop_lut.csv|||||Unit of Sally Downs Supersuite.|Includes MONZOGRANITE: Dillinger, Kevins Dam, Koondooloo, Loadstone, Magotty Springs; Mount Christine Granite, Shepherds Bore Granite, Violet Valley Tonalite.|||
31898|Kevins Dam Suite|70154|6|Mentioned|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Also contains Koondooloo Monzogranite, Magotty Springs Monzogranite, Shepherds Bore Granite, Violet Valley Tonalite, Wesley Yard Monzogranite, Loadstone Monzogranite. |1808 Ma|Sally Downs Supersuite|Includes Mount Christine Granite, Dillinger Monzogranite, Kevins Dam Monzogranite|||
31898|Kevins Dam Suite|70812|4|Described|p8|Orosirian|Orosirian|Lamboo Province, most commonly in the Central Zone although units occur throughout the whole length of the province. Interpreted to have formed over a west or northwest dipping subduction zone in the Halls Creek orogeny. Misspelt as the Kevins Dams Suite on p8.|c. 1835-1805 Ma|Sally Downs Supersuite||||
31898|Kevins Dam Suite|70851|5|Briefly described|p5|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province.||Sally Downs Supersuite|||Granitic rocks.|
31898|Kevins Dam Suite|71113|5|Briefly described|p101|Orosirian|Orosirian|Geological province: Central Zone, Lamboo Province, Halls Creek Orogen. Formed from collision of North American and Kimberley cratons (Sheppard et al., 2001).||Unit of Sally Downs Supersuite.||||
31898|Kevins Dam Suite|71140|6|Mentioned|p101|Orosirian|Orosirian|Lamboo Province, Halls Creek Orogen. Probably formed after the suturing of Kimberley and North Australian Cratons.||Sally Downs Supersuite.|||High-K granites.|
31898|Kevins Dam Suite|71267|6|Mentioned|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma).||Unit of Sally Downs Supersuite.|Includes Kevins Dam, Dillinger , Koondooloo, Magotty Springs, Westley Yard and Loadstone monzogranites, Mount Christine and Shepherds Bore granites, Violet Valley Tonalite.|||
31898|Kevins Dam Suite|71397|5|Briefly described|p6|Orosirian|Orosirian|Geological province: Central Zone, Lamboo Province, Halls Creek Orogen.|1827-1808 Ma|Unit of Sally Downs Supersuite.||||
31898|Kevins Dam Suite|71873|5|Briefly described|p427|Orosirian|Orosirian|Geological province: Lamboo Province. Emplaced within Koongie Park Formation during Halls Creek Orogeny (Page and Hancock, 1988).|1827-1808 Ma|Unit of Sally Downs Supersuite.||Intruded into Koongie Park Formation.||
35607|Kiaki Monzogranite|23582|5|Briefly described|Map Legend|Archean|Archean|Leucomonzogranite, typically deeply weathered; includes hornfelses Mount Belches Formation.||||||07-NOV-08
35607|Kiaki Monzogranite|23584|5|Briefly described|p19|||See also page 7, Fig 3. Geological Province: Yilgarn Craton.||||||
35607|Kiaki Monzogranite|65264|5|Briefly described|p21, p47 Appdx. 1|Archean|Archean|Intruded the Mount Belches Formation - causing graded wacke-mudstone units to be hornfelsed, or metasomatised. Leucoonzogranite, typically deeply weathered.||||||07-FEB-11
35607|Kiaki Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton. Ages obtained may be interpreted in two ways. Crystallisation age may be 2692+/-8 Ma, or 2666+/-6 Ma. See geochron file 177914.1.pdf (2007).||||Intrudes Mount Belches Formation?|Leucomonzogranite, typically deeply weathered; intrudes and hornfelses rocks of the Mount Belches Formation.|06-AUG-15
35607|Kiaki Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|||||Intrudes Mount Belches Formation.|Leucomonzogranite, typically deeply weathered;|
35607|Kiaki Monzogranite|70802|5|Briefly described|100k_geologyp10_lut.csv + geochron files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Sample GSWA 177914 (leucocratic monzogranite) yielded a weighted mean 207Pb*/206Pb* date of 2692+\-8 Ma, interpreted as either age of contact metamorphism with the Mount Belches Formation, or igneous crystallisation age of Kiaki Monzogranite.|||||Leucomonzogranite, typically deeply weathered; intrudes and hornfelses rocks of the MOUNT BELCHES FORMATION|
35607|Kiaki Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
35607|Kiaki Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Intrudes and hornfelses rocks of the Mount Belches Formation. Sample GSWA 177914 (leucocratic monzogranite) yielded weighted mean 207Pb/206Pb ages of 2692+\-8 Ma and 2666+\-6 Ma. If the Kiaki Monzogranite is coeval with granitic rocks responsible for contact metamorphism of the c. 2660 Ma Mount Belches Formation, then the c. 2692 Ma age may represent xemocrystic zircon components, and the c. 2666 Ma would represent zircon growth during igneous crystallisation. If the Kiaki Monzogranite is not coeval with the rocks that metamorphosed the Mount Belches Formation, then the c. 2692 Ma age may represent the igneous crystallisation age, and the c. 2662 Ma zircons may represent metamorphic zircon growth. See 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|||||Leucomonzogranite, typically deeply weathered.|
35001|Kialrah Rhyolite|23046|5|Briefly described|175|||Age: 2970 Ma.||||||26-JUL-07
35001|Kialrah Rhyolite|23244|5|Briefly described|p22||| Age: SHRIMP U-Pb zircon age of 2972+/-2Ma. of Pilbara Craton.||||||
35001|Kialrah Rhyolite|23348|5|Briefly described|222|Archean|Archean|Age: 2972+/-2Ma.||||||07-NOV-08
35001|Kialrah Rhyolite|23484|4|Described|p10 table 3|Archean|Archean|Age: 2972 +/- 2 Ma.  Maximum thickness: 1000m.  Geological Province: Mallina Basin.||||||07-NOV-08
35001|Kialrah Rhyolite|23598|5|Briefly described|p10|Archean|Archean|Age: c.2970 Ma. See also page 5 Figure 3. Underlain by Louden Volcanics. Geological Province: Pilbara Craton.||||||07-NOV-08
35001|Kialrah Rhyolite|23743|5|Briefly described|p2 Fig 1|||Geological Province: Pilbara Craton.||||||
35001|Kialrah Rhyolite|23789|5|Briefly described|p17 Fig. 4|||Geological Province: Mallina Basin.||||||
35001|Kialrah Rhyolite|23793|4|Described|p28|Archean|Archean|Of Bookingarra Group.||||||07-NOV-08
35001|Kialrah Rhyolite|23794|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup. Geological Province Pilbara Craton.||||||07-NOV-08
35001|Kialrah Rhyolite|23813|5|Briefly described|p116|Archean|Archean|Age: 2.97Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.  See also p90 Tb. 1.||||||07-NOV-08
35001|Kialrah Rhyolite|23936|5|Briefly described|Tb.1|Archean|Archean|Age: c.3.0-2.925 Ga. Geological Province: Pilbara Craton. Underlain by Louden Volcanics.||||||07-NOV-08
35001|Kialrah Rhyolite|24023|4|Described|p20|Archean|Archean|Of Bookingarra Group. Geological Province: Pilbara Craton. Maximum Thickness: 1000m.||||||07-NOV-08
35001|Kialrah Rhyolite|24024|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
35001|Kialrah Rhyolite|24140|5|Briefly described|p215|Archean|Archean|Intrudes or overlies Negri Volcanics. Age: 2975+/-4Ma (Nelson 1998).||||||07-NOV-08
35001|Kialrah Rhyolite|24184|4|Described|p715|Archean|Archean|Of the Bookingarra Group. Overlain by Louden Volcanics. Geological Province: Mallina Basin. Max depositional age: 2975 +/- 4Ma. Overlies the Louden and Negri Volcanics.||||||17-MAR-09
35001|Kialrah Rhyolite|24191|5|Briefly described|p829|Archean|Archean|Of Bookingarra Group. Overlies Louden Volcanics. Geological Province: Pilbara Craton.||||||07-NOV-08
35001|Kialrah Rhyolite|24353|4|Described|p5|Archean|Archean|Underlain by Louden Volcanics. Age: c.2970Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
35001|Kialrah Rhyolite|24550|5|Briefly described|p36 Tb. 3.2|Archean|Archean|Of the Bookingarra Group. Rhyolite. Age: ca 2975+/-4 Ma (Nelson 1998a). Geological Province: Pilbara Craton.||||||07-FEB-11
35001|Kialrah Rhyolite|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Age: >2.9Ga. Geological Province: Pilbara Craton.||||||07-NOV-08
35001|Kialrah Rhyolite|63420|5|Briefly described|Map legend|Archean|Archean|Of the Croydon Group (Pilbara Supergroup). Age: 2941Ma. Geological Province: Pilbara Craton. Flow-banded porphyritic rhyolite and minor dacite; metamorphosed.||||||07-NOV-08
35001|Kialrah Rhyolite|63441|4|Described|p5 Tb.1, p27|Archean|Archean|Of Croydon Group (Pilbara Supergroup). Overlies the Bookingarra Formation. Age: 2943+/-7Ma. Geological province: Mallina Basin, Pilbara Craton. Thick, metamorphosed, flow-banded and porphyritic rhyolite.||||||07-FEB-11
35001|Kialrah Rhyolite|63538|4|Described|p6 Fig. 3|Archean|Archean|Of Croydon Group. Underlain by Bookingarra Formation and Constantine Sandstone. Geological Province: Pilbara Craton. Felsic volcanic rocks.||||||19-APR-13
35001|Kialrah Rhyolite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Croydon Group (De Grey Supergroup). Age: c.2943Ma.  Geological province: Mallina Basin. Flow-banded porphyritic rhyolite and minor dacite; metamorphosed.||||||07-NOV-08
35001|Kialrah Rhyolite|64580|4|Described|map legend||Mesoarchean|Of Croydon Group. Flow banded porphyritic rhyolite and minor dacite; metamorphosed.||||||15-DEC-08
35001|Kialrah Rhyolite|66217|5|Briefly described|p39, p42.|Mesoarchean|Mesoarchean|Mallina Basin.|c.2940 Ma.|Unit in Croydon Group.|||Felsic volcanics.|
35001|Kialrah Rhyolite|67201|4|Described|p7 Fig.4, p21 Fig.12, p57|||In northwestern Pilbara Craton, De Grey Superbasin, West Pilbara Superterrane and East Pilbara Terrane, Mallina Basin.|Max dep age 2943+/-7 Ma, GSWA 144261|Croydon Group||Overlies Mount Negri Volcanic Member (Bookingarra Formation).|Rhyolite.|24-NOV-16
35001|Kialrah Rhyolite|68283|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Mallina and Lalla Rookh Basins.|c. 2948 Ma|Of the Croydon Group.|||Flow-banded porphyritic rhyolite and minor dacite; metamorphosed.|
35001|Kialrah Rhyolite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Croydon Group|||Flow-banded porphyritic rhyolite and minor dacite; metamorphosed|
35001|Kialrah Rhyolite|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological Province: West Pilbara Granite-Greenstone Terrane, Central Pilbara Tectonic Zone, and southwest Pilbara inlier, Pilbara Craton.|c. 2945 Ma|Unit of Croydon Group.|||Flow banded porphyritic rhyolite and minor dacite; metamorphosed|
35001|Kialrah Rhyolite|69299|5|Briefly described|p6 Tb.1|Archean|Mesoarchean|Thickness on COOYA POOYA: 0-1000 m.|Maximum age c. 2975 Ma.|Of Bookingarra Group.||Overlies or intrudes Louden Volcanics.|Feldspar-phyric, commonly flow-banded rhyolite.|
35001|Kialrah Rhyolite|69300|5|Briefly described|map legend|Archean|Archean|Mallina Basin, Whim Creek greenstone belt.|Isotopic age <2975 Ma (Nelson 1998)|Bookingarra Group|||Flow-banded porphyritic rhyolite and dacite; metamorphosed|02-SEP-14
35001|Kialrah Rhyolite|69301|5|Briefly described|p5 Fig.3|||Pilbara Craton. West Pilbara Superterrane and East Pilbara Terrane. Mallina Basin.||Croydon Group|||Felsic volcanic rocks.|
35001|Kialrah Rhyolite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton. Of Mallina Basin, De Grey Superbasin. Events: North Pilbara Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|2948-2941 Ma (isotopic)|Unit of Croydon Group.|||Flow-banded porphyritic rhyolite and minor dacite; metamorphosed|
35001|Kialrah Rhyolite|70022|6|Mentioned|p115|||West Pilbara Superterrane.||||||
35001|Kialrah Rhyolite|70775|5|Briefly described|p29 tbl 5, p41|Mesoarchean|Mesoarchean|Mallina Basin. An age range of 2948-2941 Ma is given in the Whim Creek Greenstone Belt. A minimum age of 2943 +/- 7 Ma is given (Nelson, 1998v). This unit is 1000m thick. See also p46, p51, p54, p60-p62, p70, p95-p96.|c. 2940 Ma (Smithies et al 2007a)|Bookingarra Group||Overlies (or intrudes) the Louden Volcanics.|Flow-banded and porphyritic rhyolite.|
35001|Kialrah Rhyolite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dacite, rhyolite|
35001|Kialrah Rhyolite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mallina Basin.|Max age 2948+/-3 Ma, min 2941+/-4 Ma.|Croydon Group|||Flow-banded porphyritic rhyolite and minor dacite; metamorphosed.|
35001|Kialrah Rhyolite|72251|5|Briefly described|p54|||Geological province: West Pilbara Superterrane, Pilbara Craton.||||Contemporaneous with Sisters Supersuite.||
35001|Kialrah Rhyolite|72668|5|Briefly described|p4, p14-15|||West Pilbara Superterrane, East Pilbara Terrane. Dated but has a variety of zircon age populations including ones derived from basement rocks.|2943 +/- 7 Ma (Pb-Pb, max dep age)|Croydon Group.||Overlies the Bookingarra Formation.||13-JAN-22
27174|Kiangi Creek Formation|22694|5|Briefly described|p8|||Edmund Subgroup, Bangemall Basin||||||
27174|Kiangi Creek Formation|22905|5|Briefly described|p52 Fig. 2, p53 Table 1, p54|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group.  Base is marked by Terrys Camp Member.  Siltstone with interbedded turbidite sandstone. Overlying unit: Munthara Formation; underlying unit: Cheyne Springs Formation.  Max. thickness: 550m.||||||24-JAN-06
27174|Kiangi Creek Formation|23280|6|Mentioned|Table1p1085|||||||||
27174|Kiangi Creek Formation|23310|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of Bangemall Group.||||||
27174|Kiangi Creek Formation|23311|5|Briefly described|map legend|Proterozoic|Proterozoic|Of Bangemall Group.||||||
27174|Kiangi Creek Formation|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Bangemall Group.||||||
27174|Kiangi Creek Formation|23403|4|Described|p7|Mesoproterozoic|Mesoproterozoic|Consists of quartz arenite beds with less common shale, siltstone, dolomite and conglomerate.||||||
27174|Kiangi Creek Formation|23485|4|Described|p31|Paleoproterozoic|Paleoproterozoic|Of Edmund Group.||||||07-NOV-08
27174|Kiangi Creek Formation|23723|4|Described|p9 Table 1|Mesoproterozoic|Mesoproterozoic|Incorporated into the West Creek Formation. Of Bangemall Group. O'lying unit Jillawarra Formation. U'lying unit Glen Ross Shale Member. Geol. Province: Bangemall Basin. Max. thickness: 1800 m.||||||
27174|Kiangi Creek Formation|24115|4|Described|p4 Fig.2, p5|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group. Age: c. 1060 Ma (Rb-Sr). Maximum Thickness: 550m. Overlies the Cheyne Springs Formation. Overlain by the Muntharra Formation. Geological Province: Edmund Basin.||||||
27174|Kiangi Creek Formation|24183|2|Defined|p1, p12, p13|Calymmian|Statherian|Disconformably overlies the Cheyne Springs Formation. Overlain by the Muntharra or Discovery Formations. Max. Thickness: 550m. Contains Stromatolites. Age: 1620-1462 Ma.||||||21-MAR-11
27174|Kiangi Creek Formation|24544|4|Described|p44 Fig.32|Mesoproterozoic|Mesoproterozoic|Of Edmund Group. Overlies Cheyne Springs Formation. Overlain by Muntharra Formation.||||||
27174|Kiangi Creek Formation|29845|6|Mentioned|p196|||||||||
27174|Kiangi Creek Formation|29916|4|Described|p115|||||||||
27174|Kiangi Creek Formation|30363|6|Mentioned|p6|||||||||
27174|Kiangi Creek Formation|30881|4|Described|p525|||||||||
27174|Kiangi Creek Formation|30884|6|Mentioned|p156|||||||||
27174|Kiangi Creek Formation|32720|6|Mentioned|Table 1|||||||||
27174|Kiangi Creek Formation|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
27174|Kiangi Creek Formation|34066|4|Described|p11|||Mid.Prot.||||||
27174|Kiangi Creek Formation|34124|5|Briefly described|Table 1|||Proterozoic. See also PP7-9,14||||||
27174|Kiangi Creek Formation|35639|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27174|Kiangi Creek Formation|35982|6|Mentioned|p136|||||||||
27174|Kiangi Creek Formation|36551|6|Mentioned|p101|||||||||
27174|Kiangi Creek Formation|36884|3|Fully described|p153|||||||||
27174|Kiangi Creek Formation|36902|6|Mentioned|p16|||||||||
27174|Kiangi Creek Formation|37024|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27174|Kiangi Creek Formation|37213|5|Briefly described|p22|||||||||
27174|Kiangi Creek Formation|37328|6|Mentioned|p4|||||||||
27174|Kiangi Creek Formation|37460|4|Described|Table 3.VI|||||||||
27174|Kiangi Creek Formation|38298|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27174|Kiangi Creek Formation|38299|4|Described|p9|||||||||
27174|Kiangi Creek Formation|38482|6|Mentioned|p16|||See also Table 5.||||||
27174|Kiangi Creek Formation|38988|6|Mentioned|p12|||||||||
27174|Kiangi Creek Formation|39171|6|Mentioned|p80|||||||||
27174|Kiangi Creek Formation|39210|5|Briefly described|Table 2|||||||||
27174|Kiangi Creek Formation|39370|4|Described|p31|||||||||
27174|Kiangi Creek Formation|40088|6|Mentioned|p226|||||||||
27174|Kiangi Creek Formation|40089|2|Defined|p24|Mesoproterozoic|Mesoproterozoic|||||||
27174|Kiangi Creek Formation|40899|6|Mentioned|Fig.1|||||||||
27174|Kiangi Creek Formation|40900|6|Mentioned|p34|||||||||
27174|Kiangi Creek Formation|41144|6|Mentioned|Table 1|||||||||
27174|Kiangi Creek Formation|41360|6|Mentioned|p192|||||||||
27174|Kiangi Creek Formation|42013|5|Briefly described|Map Legend|Proterozoic||||||||
27174|Kiangi Creek Formation|42471|4|Described|p20|||||||||
27174|Kiangi Creek Formation|42472|5|Briefly described|Map legend|||||||||
27174|Kiangi Creek Formation|44142|4|Described|p313 Tb.4-4, p317-320, p326 Tb.4-5|||700-2000m thick high-energy barrier bar/beach; delta-front marine deposits. Within Florry Subgroup of Chuck (1984).||Edmund Subgroup.|Glen Ross Shale Member (in Mt Vernon Syncline).|Overlies Cheyne Springs and Irregully Formations (both conformably).  Overlain by and part equivalent to Jillawarra Formation.|Quartz arenite, shale, siltstone; minor dolomite, conglomerate.|13-MAR-18
27174|Kiangi Creek Formation|44319|14|Not recorded|map legend||Mesoproterozoic|Bangemall Group. M.Proterozoic.||||||
27174|Kiangi Creek Formation|44481|5|Briefly described|map legend||Mesoproterozoic|||||||
27174|Kiangi Creek Formation|50188|6|Mentioned|p14|||Of the Edmund Group. Unit with a shale component.||||||16-JUL-08
27174|Kiangi Creek Formation|50225|4|Described|p387 Fig. 2, p394|||Of the Edmund Group (Bangemall Supergroup). Consists mainly of deep shelf siltstone and interbedded turbiditic sandstone. Unconformably overlies Cheyne Springs, Blue Billy or Irregully Formations.  Max. thickness: 550m.||||||07-FEB-11
27174|Kiangi Creek Formation|50226|5|Briefly described|p428|||Of the Edmund Group.  Has mineralised horizons.||||||
27174|Kiangi Creek Formation|50292|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Geological Province: Edmund Basin.  Of the Edmund Group (Bangemall Supergroup). Overlies: Cheyne Springs Formation, Blue Billy Formation.||||||07-NOV-08
27174|Kiangi Creek Formation|50312|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Edmund Group. Overlain by Discovery Formation. Geological Province: Edmund Basin. Thin to very thick bedded quartz sandstone, and siltstone and mudstone; minor dolostone and conglomerate.||||||31-MAY-04
27174|Kiangi Creek Formation|50313|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup).  Geological Province: Edmund Basin. Underlies: Discovery Formation.  Overlies: Cheyne Springs Formation.||||||07-NOV-08
27174|Kiangi Creek Formation|50380|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin.||||||07-NOV-08
27174|Kiangi Creek Formation|60301|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin. Siltstone and mudstone, quartz sandstone and minor conglomerate.||||||07-NOV-08
27174|Kiangi Creek Formation|62428|6|Mentioned|p346|||Sandstone and shale unit in the Gascoyne Complex.||||||
27174|Kiangi Creek Formation|63469|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Of Edmund Group. Undivided; siltstone, mudstone, and thin- to thick-bedded quartz sandstone; minor conglomerate.||||||24-SEP-07
27174|Kiangi Creek Formation|63470|5|Briefly described|Map legend|||Of the Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin. Siltstone, mudstone and thin to very thick bedded quartz sandstone; minor dolostone and conglomerate.||||||24-SEP-07
27174|Kiangi Creek Formation|63471|5|Briefly described|Map legend|||Of the Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin. Siltstone, mudstone and thin- to very thick-bedded quartz sandstone; minor dolostone and conglomerate.||||||24-SEP-07
27174|Kiangi Creek Formation|63866|4|Described|p162|Calymmian|Statherian|SHRIMP U-Pb zircon ages are detrital and interpreted as representing the maximum age of deposition for this formation; however, regional stratigraphic and intrusive relationships suggest an age ranging from about 1620-1465 Ma. An additional age of 1782 +/- 13 Ma is derived from Cawood and Nemchin, 2002.|1798 +/- 12 Ma (Nelson, 2002) |Edmund Group|||Sandstones.|
27174|Kiangi Creek Formation|63869|5|Briefly described|p24, p28, p29, p30, p31, p32-34, p45|Calymmian|Statherian|See also p59-60, Plate 1. 200-550 m thick. Contains local disseminations of copper oxides, and minor zinc.||Unit in Edmund Group.||Disconformably overlies Cheyne Springs, Blue Billy and Irregully Formations. Is overlain by Muntharra or Discovery Formations.|A succession of interbedded planar-laminated siltstone and thin- to thick-bedded sandstone; minor conglomerate and dolostone.|
27174|Kiangi Creek Formation|64283|5|Briefly described|p53|||Of the Edmund Group (Bangemall Supergroup).||||||07-FEB-11
27174|Kiangi Creek Formation|64580|4|Described|map legend||Mesoproterozoic|Of Edmund Group. Siltstone and mudstone; sandstone, and dolostone, minor conglomerate.||||||09-DEC-08
27174|Kiangi Creek Formation|64728|5|Briefly described|p96 Fig.3, p98, p104.|Mesoproterozoic|Mesoproterozoic|Shallow-to deep-marine siliciclastic and carbonate facies.|Maximum age of deposition around c.1799-c.1681 Ma.|||Unconformably overlies Cheyne Springs Formation. Is overlain by Muntharra Formation.|Medium- to thick-bedded, fine-grained sandstone; includes a distinctive unit of conophyton stromatolites near the base.|
27174|Kiangi Creek Formation|65450|5|Briefly described|p3-6|Mesoproterozoic|Mesoproterozoic|Intruded by Narimbunna Dolerite sills dated at 1465 Ma. Associated with Au mineralisation.|Age min: 1465 Ma.|Edmund Group.||Intruded by Narimbunna Dolerite sills.|Sandstone, chert, siltstone.|05-JAN-17
27174|Kiangi Creek Formation|65453|5|Briefly described|map legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group. Over Irregully Formation; under Discovery Formation. Siltstone, mudstone, quartz sandstone; minor dolostone and conglomerate. Geol. Prov: Edmund Basin.||||||
27174|Kiangi Creek Formation|65545|5|Briefly described|Map Legend|Mesoprotoerozoic|Paleoproterozoic|Of Edmund Group, Edmund Basin. Age: c. 1460 - <1620 Ma. Siltstone and mudstone, and thin to very thick-bedded quartz sandstone; minor dolostone and conglomerate.||||||
27174|Kiangi Creek Formation|65549|5|Briefly described|Map Legend|Calymmian|Statherian|Of Edmund Group, Bangemall Supergroup, Edmund Basin. Underlies Discovery Formation; overlies Irregully Formation. Siltstone, mudstone, and thin- to very thick-bedded quartz sandstone; minor dolostone and conglomerate. ||||||
27174|Kiangi Creek Formation|65830|4|Described|p4-7, p10, p12-16, p19-21; Plates 1,2|Calymmian|Statherian|200m to 500m thick. Shallow to deeper marine-shelf deposit. Contains Conophyton stromatolites.||Of the Edmund Group||Disconformably overlies Irregully, Gooragoora, Cheyne Springs, Blue Billy Formations. Conformably overlain by the Muntharra and Discovery Formations.|Interbedded siltstone and sandstone; local stromatolitic dolostone and conglomerate.|
27174|Kiangi Creek Formation|65896|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in Edmund Group, Bangemall Supergroup. Planar-laminated, ferruginous siltstone and shale, and cross-bedded, medium-grained, quartz sandstone.Includes unnamed chert member.||||||
27174|Kiangi Creek Formation|66104|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in Edmund Group. Siltstone, mudstone, and thin to very thick bedded quartz sandstone; minor dolostone and conglomerate (not on map).||||||
27174|Kiangi Creek Formation|66105|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund Group. Overlies Irregully Formation; underlies Discovery Formation. Siltstone, mudstone, quartz sandstone; minor dolostone and conglomerate. Includes two unnamed units; thick-bedded sandstone and siltstone; siltstone with fine-grained sandstone.||||||
27174|Kiangi Creek Formation|66110|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in Edmund group. Siltstone, minor fine-grained sandstone; interbedded metasiltstone and fine-grained metasandstone.||||||
27174|Kiangi Creek Formation|66112|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in Edmund Group. Siltstone, mudstone, and thin- to very thick-bedded quartz sandstone; minor dolostone and conglomerate (not on map). Includes mapped but unnamed units of chert, ferruginous  siltstone, minor fine-grained sandstone.||||||
27174|Kiangi Creek Formation|66241|4|Described|pp1-6, p7, pp9-12, pp28-29.  |||The lower part of this unit correlates with the West Creek Formation; the upper part with Jillawarra Formation. In the Jillawarra sub-basin, this unit equates to rocks previously mapped as the Coobarra, Kiangi Creek, and Jillawarra Formations by Muhling and Brakel (1985) and the West Creek and Jillawarra Formations by Vogt (1995). A 0.2 to 2.6 km thick succession of fine-grained siliciclastic and carbonate sedimentary rocks. Hosts the Abra polymetallic deposit.||Unit in Edmund Group.|Includes Tangadee Rhyolite.|Disconformably overlies Cheyne Springs Formation. Is intruded by ?Narimbunna Dolerite sills. Is overlain conformably by Muntharra Formation, and ?disconformably by Discovery Formation.|Fluvial sandstone and conglomerate; fan-delta sandstone and siltstone; interbedded rhyolite.|
27174|Kiangi Creek Formation|66299|4|Described|p232, pp299-303.|Mesoproterozoic|Mesoproterozoic|Low to medium grade metamorphosed; commonly silicified.|1619-1460 Ma.|Unit in Edmund Group.||In faulted contact with all older lithologies including Halfway Gneiss; Moogie, Leake Spring Metamorphics; Moorarie, Durlacher Supersuites. Overlain by younger Edmund Group units.|Interbedded metasiltstones and fine-grained metasandstones.|
27174|Kiangi Creek Formation|67136|5|Briefly described|Map legend.|||Edmund Basin.||Unit in Edmund Group.||Overlies Blue Billy Formation and Irregully Formation. Is overlain by Discovery Formation.|Siltstone, mudstone, and thin- to very thick-bedded quartz sandstone; minor dolostone and conglomerate.|14-NOV-11
27174|Kiangi Creek Formation|67245|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Edmund Basin. Includes seven other separately-mapped but un-named sub-units. ||Unit in Edmund Group.||Overlies Irregully Formation. Is intruded by Narimbunna Dolerite. Is overlain by Discovery Formation.|Siltstone, mudstone, and thin- to very thick-bedded quartz sandstone; minor dolostone and conglomerate, ferruginous siltstone commonly manganiferous.|
27174|Kiangi Creek Formation|67246|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Edmund Basin. Includes six un-named sub-units which are mapped separately.||Unit in Edmund Group.||Overlies Irregully Formation. Is intruded by Narimbunna Dolerite. Is overlain by Discovery Formation.|Siltstone, mudstone, and thin- to very thick-bedded quartz sandstone; minor dolostone and conglomerate.|19-NOV-13
27174|Kiangi Creek Formation|67247|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Edmund Basin.. Shown as part of 'Depositional package 3' in the interpreted bedrock geology map legend.||Unit in Edmund Group.||||20-NOV-13
27174|Kiangi Creek Formation|67269|6|Mentioned|p20-21 Fig.19|||Bangemall Basin. Contains Conophyton new form stromatolites with an axial zone; photograph shown to demonstrate the continuity of such zones through geological time, and to support the biogenic origin of stromatolitic structures in Strelley Pool Formation (East Pilbara Terrane).||Edmund Group.||||
27174|Kiangi Creek Formation|67346|5|Briefly described|p795 Fig.2, p796 Fig.3|Calymmian|Calymmian|Minimum age from age of Narimbunna Dolerite. Maximum age from Edmund Group age.||Of the Edmund Group.||Intruded by Narimbunna Dolerite.|Includes siltstone and sandstone.|11-MAY-12
27174|Kiangi Creek Formation|67374|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Edmund Basin.||Unit in Edmund Group.|||Siltstone, mudstone, and thin- to very thick-bedded quartz sandstone; minor dolostone and conglomerate.|
27174|Kiangi Creek Formation|68280|6|Mentioned|p26 fig 24|||Bangemall Basin.||Edmund Group||||
27174|Kiangi Creek Formation|68285|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin.||Of the Edmund Group.|Informally subdivided in part into three unnamed units.|Underlain by Cheyne Springs Formation, Blue Billy Formation or Irregully Formation. Overlain by the Discovery Formation.|Siltstone, mudstone, and thin to very thick bedded quartz sandstone; minor dolostone and conglomerate; siltstone; minor fine-grained sandstone; dolostone, siltstone, and sandstone; medium to very thick bedded quartz sandstone and siltstone.|
27174|Kiangi Creek Formation|68286|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin.||Of the Edmund Group|Informally subdivided in part into five unnamed units.|Underlain by the Cheyne Springs Formation. Overlain by the Discovery Formation.|Siltstone, mudstone, and thin to very thick bedded quartz sandstone; minor dolostone and conglomerate; chert.|
27174|Kiangi Creek Formation|68521|5|Briefly described|Map Legend|Calymmian|Statherian|||Of the Edmund Group.|||Siltstone; minor fine-grained sandstone.|
27174|Kiangi Creek Formation|68522|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin.|<1620 - c.1465 Ma|Of the Edmund Group.|||Siltstone; minor fine-grained sandstone.|
27174|Kiangi Creek Formation|69003|5|Briefly described|p34, p42|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen. Hosts the giant Abra polymetallic deposit (described).||Edmund Group.||Unconformably overlies Cheyne Springs Formation. Is overlain by Muntharra Formation.||
27174|Kiangi Creek Formation|69024|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin. Includes a separately mapped, unnamed subunit of medium to very thick bedded quartz sandstone and siltstone.||Of the Edmund Group.|||Siltstone, mudstone, and thin to very thick bedded quartz sandstone; minor dolostone and conglomerate.|05-MAY-14
27174|Kiangi Creek Formation|69027|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin. Includes 3 unnamed subunits mapped separately, comprising medium to very thick bedded quartz sandstone and siltstone; dolostone, siltstone, and sandstone; and siltstone (minor fine-grained sandstone).||Of the Edmund Group.||Underlain by the Cheyne Springs Formation.|Siltstone, mudstone, and thin to very thick bedded quartz sandstone; minor dolostone and conglomerate.|05-MAY-14
27174|Kiangi Creek Formation|69028|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin. Mapped with Muntharra Formation as one unit.||Of the Edmund Group.|||Siltstone and mudstone, sandstone, and dolostone; minor conglomerate.|06-MAY-14
27174|Kiangi Creek Formation|69166|4|Described|geologyp_lut.csv|Mesoproterozoic|Paleoproterozoic|Age derived from quartz sandstone and a feldspathic quartz sandstone sample with an age of 1798Ma  +/-12 Ma (148973.1.pdf, 169061.1.pdf)|1682 +/- 18 Ma   (SHRIMP)|Edmund Group||Unconformably overlies Irregully Formation, Overlain by Muntharra Formation, Discovery Formation|Chert, siltstone, dolostone, sandstone, interbedded metasiltstone and fine grained metasandstone. Conglomerate, pebbly sandstone, quartz sandstone, ferruginous siltstone, silicified feldspathic quartz sandstone.|
27174|Kiangi Creek Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|||Part of Edmund Group, Depositiional package 3.||Unit of Edmund Group.||||
27174|Kiangi Creek Formation|69387|6|Mentioned|p31|||Gravity and magnetic modelling.||||||
27174|Kiangi Creek Formation|69596|6|Mentioned|p12 Fig.7|||Edmund Basin.||Edmund Group.||||
27174|Kiangi Creek Formation|70019|4|Described|p92-96,108-109|Mesoproterozoic|Mesoproterozoic|Geological province: Gascoyne Province, Capricorn Orogen. Reflects the interrelationship of a coarse-grained allucvial system to the east, and a rapidly subsiding fault-bound marine depocentre to the west. Comprises a lower fluvial, alluvial-fan facies (40m thick), an upper deltaic to deep marine facies (up to 1.3 km thick), separated by an erosional MFS. Intruded by Tangandee Rhyolite. Hosts main mineralisation of the Abra polymetallic (Fe, Pb, Zn, Ba, Cu, Au, Ag, Bi, and W) deposit within the lower alluvial-fan facies. Upper marine facies contain isolated barite-chalcopyrite-dolomite-galena veins, suggesting a second phase of post-depositional mineralisation. Approximate time-gap of 20My between c. 16210 and 1590 Ma between upper and lower facies of Kiangi Creek Formation. ||Unit of Edmund Group.||Overlain by Muntharra Formation. Underlain by Cheyne Springs Formation.|Lower facies: alluvial-fan sandstones and conglomerate, local small lenticular rhyolite bodies, felsic volcanics. Upper facies: siltstone interbedded with massive to graded, fine- to very coarse-grained sandstone and minor conglomerate.|
27174|Kiangi Creek Formation|70127|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Edmund Group.|||Siltstone and thin- to thick-bedded sandstone; minor conglomerate.|
27174|Kiangi Creek Formation|70132|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Edmund Basin. The two facies are mapped separately.||Edmund Group.||Overlies Irregully Formation. Is overlain by Discovery Formation.|Medium- to very thick-bedded quartz sandstone and siltstone; siltstone with minor fine-grained sandstone, dolostone and chert.|
27174|Kiangi Creek Formation|70138|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin. The two facies are mapped separately.||Edmund Group.||Overlies Gooragoora Formation. Is intruded by Narimbunna Dolerite. Is overlain by Discovery Formation.|Siltstone and thin- to thick-bedded sandstone, minor conglomerate; siltstone, minor fine-grained sandstone, dolostone and chert.|
27174|Kiangi Creek Formation|70767|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin. Section only: no outcrop in map area.||Edmund Group.||Overlies Irregully Formation. Is overlain by Discovery Formation.|Siltstone, fine- to very coarse-grained sandstone, dolostone; minor conglomerate, chert, felsic volcanic rock. Separately mapped: medium- to very thick-bedded quartz sandstone and siltstone; siltstone, minor fine-grained sandstone, dolostone, chert.|
27174|Kiangi Creek Formation|70768|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin. Section only: no outcrop in map area.||Edmund Group.||Overlies Irregully Formation. Is overlain by Discovery Formation.|Siltstone, fine- to very coarse-grained sandstone, dolostone; minor conglomerate, chert, felsic volcanic rock. Separately mapped: medium- to very thick-bedded quartz sandstone and siltstone; siltstone, minor fine-grained sandstone, dolostone, chert.|
27174|Kiangi Creek Formation|70795|4|Described|100k_geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Also 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 143450.1.pdf, 149021.1.pdf, West Australian Craton, Edmund Basin. Also disconformably overlies Blue Billy Formation and Cheyne Springs Formation, intruded by Waldburg Dolerite.|1590-1517 Ma|Edmund Group||Overlain by Discovery Formation and Muntharra Formation, Unconformably overlies Irregully Formation and Moorarie Supersuite.|Interbedded silicified siltstone,dolostone,feldspathic quartz sandstone, sandstone, conglomerate, minor fine grained sandstone, pebbly sandstone and chert.|
27174|Kiangi Creek Formation|70814|4|Described|p3, p5, p8-p9, p11-p12|Calymmian||Edmund Basin. Together with the Muntharra Formation forms Depositional Package 3 of the Edmund Group. Up to 2600m thick and forms extensive outcrops in the Edmund Basin. On the Pingandy Shelf this unit is between 600-700m thick and consists of stromatolitic and non-stromatolitic dolomite, dolomitic siltstone, siltstone and sandstone deposited in fluvio-deltaic or shallow-marine environments. Outcrop characteristics and thicknesses in different map sheets are discussed briefly. A minimum depositional age is derived from a U-Pb zircon age of 1517 +/- 8 Ma (Wingate et al., 2015a) from the intruding Waldburg Dolerite. Overlies the Cheyne Springs Formation. Conformably overlain by the Muntharra Formation. Intruded by the Waldburg Dolerite. See also p18, p20, p22, p24-p25, p27, p33, p39, p47, p55.||Edmund Group|Includes the Tangadee Rhyolite.|Unconformably overlies the Irregully and Gooragoora Formations. Disconformably overlies the Moorarie Supersuite.|Siltstone, fine-grained to very coarse-grained sandstone, dolomite and minor conglomerate, chert and felsic volcanic rocks.|
27174|Kiangi Creek Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone, mudstone, crystalline dolostone/dolomite, dolostone|
27174|Kiangi Creek Formation|71273|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin.||Edmund Group.|||Six facies associations are separately mapped. Siltstone, sandstone, conglomerate, dolostone and chert.|16-FEB-18
27174|Kiangi Creek Formation|72259|6|Mentioned|App. Tb.B||||||||Includes laminated siltstone.|
27174|Kiangi Creek Formation|72705|5|Briefly described|p3-4|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen. Hosts polymetallic sediment-hosted mineralisation at the Abra deposit.||Edmund Group.||Unconformably overlies Cheyne Springs Formation. Is overlain by Muntharra Formation.|Conglomerate to sandstone and siltstone; deposited in alluvial fan and deep shelf environments respectively.|
27174|Kiangi Creek Formation|72758|5|Briefly described|p8 Tb.1, p50, p53.|||240m thick. Forms the prominent capping to Mount Florry.This formation along with Irregully Formation has a combined thickness of 3000m in Wyloo area.||Bangemall Group||Conformably overlies Wannery Member, Yeelingie Member of Irregully Formation.|Grey, highly silicified, quartz sandstone.|
27174|Kiangi Creek Formation|73442|6|Mentioned|p8, p18|||Also referred to as Depositional Package 3.||||Intruded by Waldburg Dolerite, Narimbunna Dolerite||
37199|Kilkenny Gabbro|23573|6|Mentioned|p11|||||||||
37199|Kilkenny Gabbro|24494|5|Briefly described|p38 App.1|||||||||
37199|Kilkenny Gabbro|65264|5|Briefly described|p22, p49 Appdx. 1|Archean|Archean|Max. thickness: ~600m. A gabbroic sill with pronounced igneous layering into a lower olivine-plagioclase zone and an upper augite-plagioclase cumulate zone.||||||07-FEB-11
37199|Kilkenny Gabbro|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton|||||Gabbro and olivine-plagioclase to pyroxene-plagioclase cumulate rocks; metamorphosed.|06-AUG-15
37199|Kilkenny Gabbro|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Gabbro and olivine-plagioclase to pyroxene-plagioclase cumulate rocks; metamorphosed.|
37199|Kilkenny Gabbro|71270|4|Described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton.|||||Gabbro and olivine-plagioclase to pyroxene-plagioclase cumulate rocks; metamorphosed|
22095|Killara Formation|7161|5|Briefly described|p90, p100|Statherian|Statherian|Age determined using detrital zircons.|1764 +/- 13 Ma detrital zircon age.||||Subalkalic to calc-alkalic tholeiites.|13-NOV-13
22095|Killara Formation|7471|5|Briefly described|p8, Map legend|Proterozoic|Proterozoic|Yerrida Basin. Formed in a rift basin.||Of the Mooloogool Subgroup.|Includes Bartle Member.|Overlies Thaduna Formation. Is overlain by Maraloou Formation.|Aphyric tholeiitic lavas and microgabbro sills.|
22095|Killara Formation|12099|4|Described|p677-681,683, 685-6, Figs.4,5,6, 9|Paleoproterozoic|Paleoproterozoic|New or redefined unit by Occhipinti et al. (1997). Outcrops in the southern, eastern and southeastern parts of the Yerrida Basin. Mafic rocks are generally unmetamorphosed, flat lying or shallow dipping, have tholeiitic to calc-alkaline basaltic and basaltic andesite compositions, and were emplaced as subaerial and subaqueous lava flows, intrusive sheets, sills and dykes. Uncertain thickness, but may be up to 1km. Pirajno and Occipinti (2000) suggest that the Killara Formation rocks are continental flood basalts.||Unit in Mooloogool Subgroup.|Includes Bartle Member.|Contact between Killara and Maraloou Formations is transitional to unconformable in the eastern Yerrida Basin. Intercalated with Doolgunna, Thaduna and Maraloou Formations.|Consists of low-Ti subalkaline intrusive and extrusive rocks with minor intercalations of silicified volcaniclastic rocks.|04-MAR-13
22095|Killara Formation|22493|6|Mentioned|p90|Statherian|Statherian|1764+/-13Ma||||||
22095|Killara Formation|22899|6|Mentioned|85|||Geol province Yerrida Basin||||||
22095|Killara Formation|22940|4|Described|Fig.1 p3|||See also Table 2 p12. of Mooloogool Subgroup, Yerrida Group.||||||
22095|Killara Formation|23133|5|Briefly described|p293 Fig.1|||of Yerrida Basin.||||||
22095|Killara Formation|23561|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Mooloogool Subgroup,Yerrida Basin||||||07-NOV-08
22095|Killara Formation|23581|5|Briefly described|Map legend||Paleoproterozoic|Of the Mooloogool Subgroup in the Yerrida Group in the Yerrida Basin||||||07-NOV-08
22095|Killara Formation|23589|4|Described|p18|||Of Mooloogool Subgroup. Overlying unit Maraloou Formation. Max. thickness 200 m.||||||
22095|Killara Formation|23593|4|Described|p11|||Of Mooloogool Subgroup. Overlying unit Marloou Formation. Underlying unit Doolgunna Formation. Geological Province: Yerrida Basin. Max. thickness ~1000 m.||||||
22095|Killara Formation|23597|5|Briefly described|p11|||Of Yerrida Group. Geological Province: Yerrida Basin.||||||
22095|Killara Formation|23600|4|Described|p11|Proterozoic|Proterozoic|Of Mooloogool Subgroup. Overlying unit Maraloou Formation. Underlying unit Doolgunna Formation. Geological Province: Yerrida Basin.||||||
22095|Killara Formation|23611|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|See also page 33 Appendix 1. Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||07-NOV-08
22095|Killara Formation|23744|5|Briefly described|p10 Table 1|Paleoproterozoic|Paleoproterozoic|Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||07-NOV-08
22095|Killara Formation|23747|5|Briefly described|p4 table 1|Paleoproterozoic|Paleoproterozoic|Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||07-NOV-08
22095|Killara Formation|23749|4|Described|p10|Proterozoic|Proterozoic|Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||
22095|Killara Formation|23750|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||
22095|Killara Formation|23865|4|Described|p170|Paleoproterozoic|Paleoproterozoic|Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||07-NOV-08
22095|Killara Formation|23890|5|Briefly described|p21 Fig.11|||Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||
22095|Killara Formation|24021|4|Described|p16|Paleoproterozoic|Paleoproterozoic|Of the Mooloogool Subgroup.   Geological Province: Yerrida Basin.||||||12-FEB-09
22095|Killara Formation|24022|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Yerrida Group. Geological Province: Yerrida Basin.||||||07-NOV-08
22095|Killara Formation|24028|4|Described|p289|Paleoproterozoic|Paleoproterozoic|Of Mooloogool Subgroup.  Geological Province: Yerrida Basin.||||||07-NOV-08
22095|Killara Formation|24535|4|Described|p1,22-28|Paleoproterozoic|Paleoproterozoic|Calc-alkaline to tholeiitic basalt and basaltic andesite. Includes volcanics and dolerite sills and dykes. ~1000m thick. Of Mooloogool Group. Geological Province: Yerrida Basin. Petrography, geochronology and magnetism described.||||Interdigitates with Thaduna  Formation and Doolgunna Formation. Intrudes all Yerrida Basin units.||26-NOV-13
22095|Killara Formation|43238|5|Briefly described|p6|||||||||
22095|Killara Formation|43836|5|Briefly described|Map Legend||Proterozoic|||||||
22095|Killara Formation|43837|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mooloogool Subgroup (Yerrida Group).||||||18-MAY-04
22095|Killara Formation|44204|5|Briefly described|Map Legend||Proterozoic|||||||
22095|Killara Formation|49893|4|Described|p13|Proterozoic|Proterozoic|Of the Mooloogool Subgroup (Yerrida Group). Geological province: Yerrida Basin. Intercalated with the Maraloou, Johnson Cairn and Thaduna Formations. See also p2 Fig.1.||||||
22095|Killara Formation|49896|5|Briefly described|p3 Tb. 2|||Of Occhipinti (1997). Located within the Mooloogool and Windplain Subgroups (Yerrida Group) - intercalated with Thaduna and Doolgunna Formations, and with Maraloou Formation.||||||13-NOV-13
22095|Killara Formation|49912|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Mooloogool Subgroup (Yerrida Group).  Undivided mafic intrusive and extrusive rocks.  Geological Province: Yerrida Basin.||||||
22095|Killara Formation|50195|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Mooloogool Group.  Age: c.1840Ma.  Geological Province: Yerrida Basin.||||||07-NOV-08
22095|Killara Formation|50216|5|Briefly described|p206|Paleoproterozoic|Paleoproterozoic|Geological Province: Yerrida Basin.||||||07-NOV-08
22095|Killara Formation|50222|4|Described|p320 Fig. 3, p322-323|Paleoproterozoic|Paleoproterozoic|Of the Mooloogool Group.  Underlies the Maraloou Formation.  Interdigitates with Doolgunna and Thaduna Formations.  Max. thickness: ~1000m.  Geological Province: Yerrida Basin.  See also p319 Fig. 2.||||||07-NOV-08
22095|Killara Formation|50223|6|Mentioned|p349|||Geological Province: Yerrida Basin.||||||
22095|Killara Formation|61271|5|Briefly described|p105 Fig.1, p106|||Of the Mooloogool Subgroup. Comprises subalkaline to calc-alkaline tholeiitic volcanic rocks, dolerite and gabbroic sills and minor pyroxenite.||||||
22095|Killara Formation|62094|5|Briefly described|p235|Paleoproterozoic|Paleoproterozoic|Of the Mooloogool Group. Includes host rocks for agate. Age: 1840Ma.||||||07-NOV-08
22095|Killara Formation|62289|4|Described|plate 1, p3, p7, p12-14, p15-29|Palaeoproterozoic|Palaeoproterozoic|Includes Bartle Member at top; of Mooloogool Subgroup (Yerrida Group); thickness: ~1000m; interdigitates with Johnson Cairn, Doolgunna and Thaduna Formations; gradationally overlain by and interfingers with Maralou Formation; subalkaline intrusive and extrusive rocks, with minor intercalations of chertified volcaniclastic rocks; previously included in Naracoota Volcanics of Gee (1987), which was subdivided into Naracoota Formation and Killara Formation by Occhipinti et al. (1997).||||||
22095|Killara Formation|62353|5|Briefly described|map legend|Proterozoic|Proterozoic|Geol. Prov: Yerrida Basin.||Of Mooloogool Subgroup, Yerrida Group.|Includes Bartle Member.|Underlies Maraloou Formation; coeval and interbedded with Thaduna and Doolgunna Formations.|Undivided mafic rocks.|14-APR-11
22095|Killara Formation|63866|5|Briefly described|p152, p165, p168, p177|||Yerrida Basin.||Mooloogool Subgroup|||Mafic extrusive and intrusive rocks.|
22095|Killara Formation|64580|4|Described|map legend||Paleoproterozoic|Of Mooloogool Group. Tholeiitic basalt; locally intercalated with dolerite sills; Chertified volcaniclastic rock and chemical sedimentary rock; Volcanic breccia; Gabbro and pyroxenite; Lithic sandstone intercalacted with tholeiitic basalt.||||||09-DEC-08
22095|Killara Formation|64772|5|Briefly described|Plate 1 legend|Paleoproterozoic|Paleoproterozoic|Included in Mooloogool Group. Age: c. 1840Ma. Geological province: Yerrida Basin.  See also p28 Fig.16, p71 App.4 Tb.4.2, p72-74 Fig.4.1.|||||Dolerite sills; locally intercalated with tholeiitic basalt|25-NOV-13
22095|Killara Formation|65264|5|Briefly described|p27, p44 Appdx. 1|||Of Mooloogool Subgp (Yerrida Gp). Contains the Bartle Member. Geol prov: Yerrida Basin. Comprises a sequence of aphyric basaltic lavas and microgabbro sills, intercalated with thin silicified volcaniclcastic rocks and nontronite layers.||||||07-FEB-11
22095|Killara Formation|65408|4|Described|pp82-83, p84 Fig.1.|Paleoproterozoic|Paleoproterozoic|Characterised by low REE abundances and trace element chemistry suggesting an intracontinental tectonic setting.||Unit in Mooloogool Subgroup.||Intercalated with Thaduna and Doolgunna Formations. Is overlain by Maraloou Formation.|Sequence of tholeiitic, aphyric lavas and microgabbro sills.|
22095|Killara Formation|65411|5|Briefly described|p88, p89 Fig.1.|Paleoproterozoic|Paleoproterozoic|||Unit in Mooloogool Subgroup.|||Mafic-ultramafic volcanic rocks of mixed continental-oceanic origin.|
22095|Killara Formation|65412|5|Briefly described|p98, p99, p101 Fig.4, p103.|Paleoproterozoic|Paleoproterozoic|Mafic igneous rocks with affinities to continental flood basalts. Is spatially associated with a positive Bouguer anomaly, suggesting a rift-related large underlying (mafic) body(ies).|||||Basaltic lavas.|
22095|Killara Formation|65418|5|Briefly described|p169.|||Pirajno and Occhipinti (1995 and in prep.) excluded a suite of mafic rock, found in the SE corner of the Peak Hill 1:250 000 map sheet, which formerly belonged to the Narracoota Volcanics (of Gee 1987, 1990; and Gee and Grey 1993), and included it in this unit.||||||21-FEB-17
22095|Killara Formation|65419|2|Defined|p4 Fig.1, p11 Fig.4, p13, pp18-23.|Paleoproterozoic|Paleoproterozoic|Named after Killara Homestead. Type area extends 25 km eastwards from 3.5 km north of the homestead. Proposed type section is from KDD1 (AMG (2745) 135772). Thickness c.1000 m. Includes some volcanic rocks previously assigned to the Narracoota Volcanics (Gee and Grey, 1993). See article for detailed synonymy.||Unit in Mooloogool Subgroup.|Includes Bartle Member.|Intrudes or overlies Finlayson Member. Interfingers with Johnson Cairn, Doolgunna and Thaduna Formations. Is overlain by Maraloou Formation.|Mafic volcanic and intrusive rocks with minor chert bands; aphyric, locally amygdaloidal, basalt lavas; extensive microgabbro sills and ?plugs; minor disseminated sulfides; chertified laminated volcaniclastic and evaporitic sediments.|
22095|Killara Formation|65472|5|Briefly described|p2, p3 Fig.2, p4|||Yerrida Basin. Age: U-Pb dating of monazite (from peperite margins of interfingering Maralou Formation and Killara Formation) (Rasmussen and Fletcher, 2002); considered a minimum depositional age for Maralou Formation and, by inference, provides a maximum age limit for deposition of overlying Yelma Formation.|c. 1.84 Ga|Of Mooloogool Group.||Interfingers with Maraloou Formation.|Mafic volcanics and intrusive rocks. Tholeiitic lavas and gabbro-dolerite sills.|24-SEP-15
22095|Killara Formation|65913|3|Fully described|p1, p2 Fig.1, p5, pp8-18.|Paleoproterozoic|Paleoproterozoic|Northeastern area of the map is a dissected plateau with dolerite outcrops characterised by spheroidally weathered boulders. Interdigitating argillaceous and arenaceous strata are assigned to the Thaduna Formation. Locally pillow lavas intercalated with sedimentary rocks of Maraloou Formation in topmost 100 m. Geochemical analysis is detailed; has a dominantly continental geochemical signature: subalkaline, basaltic andesitic, high-Fe tholeiitic. Presence of pumpellyite, prehnite and zeolites suggests very low grade metamorphism. A gold anomaly of 13 ppb was recorded near contact with Bartle Member; anomalous Pt and Pd values in stream sediments overlying this unit.||Unit in Mooloogool Subgroup.|Includes Bartle Member.|Overlies Johnson Cairn Formation. Is intercalated with Doolgunna and Thaduna Formations. Is overlain by Maraloou Formation.|Mafic igneous rocks: gabbroic intrusions, submarine (pillow) and subaerial vesicular tholeiitic basaltic lava flows, and dolerite dykes and sills; ophitic to subophitic augite microgabbro +/- orthopyroxene; capped by chert and chert brecccia.|
22095|Killara Formation|66427|6|Mentioned|p40 Fig.1|||Eruption of continental tholeiites.||||||
22095|Killara Formation|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic|||Mooloogool Group|||Tholeiitic basalt; locally intercalated with dolerite sills, and vice versa; Chertified volcaniclastic rock and chemical sedimentary rock; Volcanic breccia.|
22095|Killara Formation|69003|5|Briefly described|p11-12|||Yerrida Basin.||Mooloogool Group.|Bartle Member.|Unconformably overlies Johnson Cairn Formation. Is overlain conformably by Maraloou Formation.||
22095|Killara Formation|69152|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin [?? previously Yerrida Basin]. Dolerite sill minimum crystallisation date. See geochron file 142863.1.pdf (2002).|1652+/- 23 Ma K/Ar|Mooloogool Group|Includes Bartle Member and unnamed subunit.|Dolerite sill intrudes Juderina Formation.|Tholeiitic basalt; locally intercalated with dolerite sills.|24-SEP-15
22095|Killara Formation|69596|6|Mentioned|p9-11|||Yerrida Basin. Has distinctly different whole rock, major, trace and rare earth element chemistry from the Narracoota Formation.||Mooloogool Group.||||
22095|Killara Formation|70153|4|Described|100k_geologyp10_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop14_lut.csv and 142863.1.pdf. Yerrida Basin. Age derived from dolerite sill sample (described in some detail). Also described as a unit in the Yerrida Group.|1652 Ma +/- 23 Ma (K-Ar).|Mooloogool Group|Includes Bartle Member.|Intrudes the Juderina Formation.|Tholeiitic basalt; locally intercalated with dolerite sills; local lithic sandstone and chert breccia.|
22095|Killara Formation|70795|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|West Australian Craton, Yerrida Basin|2500-1600 Ma||||Tholeiitic basalt; locally intercalated with dolerite sills; local lithic sandstone and chert breccia.|
22095|Killara Formation|70796|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|Yerrida Basin, Capricorn Orogen. See also glengarry_100k_geologyp_lut.csv, glengarry_500k_interpgeop_lut.csv, 118990.1.pdf,|ca 25001600 Ma (inferred)|Mooloogool Group|||Tholeiitic basalt; locally intercalated with dolerite sills; local lithic sandstone and chert breccia.|
22095|Killara Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sedimentary rock, basalt, pyroxenite, basaltic andesite, dolerite|
22095|Killara Formation|71269|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Of Yerrida Basin. Events: Capricorn Orogeny (1817-1772 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, glengarry_100k_geologyp_lut.csv, glengarry_500k_interpgeop_lut.csv. Contains 1764+\-13 Ma zircons (Pb/Pb age) from shales interbedded with volcaniclastics near the base of the Killara Formation, interpreted as a maximum depositional age.|2170-1600 Ma (inferred)|Unit of Mooloogool Group.|||Tholeiitic basalt; locally intercalated with dolerite sills; local lithic sandstone and chert breccia|
22095|Killara Formation|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen. Of Earaheedy Basin. Events: Capricorn Orogeny (1817 - 1772 Ma). See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 100k_geologysub10_lut.csv.||Unit of Mooloogool Group.|Includes Bartle Member.|Intruded by a 1623+\-23 Ma dolerite sill.|Ttholeiitic basalt intercalated with dolerite sills.|
22095|Killara Formation|71468|4|Described|p24-26,30-36|Orosirian|Orosirian|Geological province: Capricorn Orogen, Yilgarn Craton. Of Yerrida Basin.||Unit of Mooloogool Group.||Overlain by, and grades into Maraloou Formation. Laterally grades into Thaduna and Doolgunna formations. Underlain by Juderina Formation.|Tholeiitic basalt locally intercalated with dolerite sills, lithic sandstone and chert breccia.|
22095|Killara Formation|71484|4|Described|p124-125,128-130,134,139|||Geological province:  Yerrida Basin. Mafic volcanics extruded and intruded into Mooloogool Sub-basin. Contains sub-volcanic dolerite sills in contact with Maraloou Formation, as evidenced by peperite margins suggesting Killara pillow basalts being extruded onto wet sediments of Maraloou Formation, and indicates partly coeval deposition.||Unit of Mooloogool Group.||Overlain by Doolgunna and Thaduna formations and Sweetwaters Well Dolomite. Underlain by, and interfingers with Johnson Cairn Formation.|Tholeiitic basalt; locally intercalated with dolerite sills; local lithic sandstone and chert breccia.|30-AUG-19
22095|Killara Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Yerrida Basin.||Mooloogool Group|||Tholeiitic basalt; locally intercalated with dolerite sills; local lithic sandstone and chert breccia.|
35397|Killi Killi Formation|23809|5|Briefly described|p16, p6 Tb. 3|||Of the Tanami Group.  Unconformably overlain by the Pargee Sandstone; overlies the Dead Bullock Formation.  Age: 1815+/-13Ma (Pb-Pb).  Intruded by Jims Find Granite and Water Tower Tonalite.Max. thickness: 4km.||||||
35397|Killi Killi Formation|50152|5|Briefly described|p71, p72 Fig. 3|||Of Tanami Group. Conformably overlies Dead Bullock Formation. Comprises turbiditic sandstone.||||||
35397|Killi Killi Formation|50315|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group.  Includes Jasperlitic Chert member.  Sandstone: purple, brown, turbiditic, thick to thin bedded micaceous and silty to quartzitic, interbedded with buff to dark grey siltstone packages; minor pebbly sandstone and chert.||||||07-NOV-08
35397|Killi Killi Formation|50374|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tanami Group. Includes Jasperlitic Chert member (informal).||||||07-NOV-08
35397|Killi Killi Formation|50376|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tanami Group. Includes the informal Jasperlitic Chert Member. Jasperlitic chert, thin bedded, rhythmically alternating pale chert and jasper, highly contorted.||||||07-NOV-08
35397|Killi Killi Formation|60676|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Tanami Group. Overlies: Dead Bullock Formation. Sandstone: turbiditic, thick to thin bedded micaceous and silty to quartzitic; interbedded with siltstone packages, pebbly sandstone and chert; volcanic lithics.||||||07-NOV-08
35397|Killi Killi Formation|60681|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Tanami Group.  Sandstone, siltstone.||||||
35397|Killi Killi Formation|61246|6|Mentioned|p19|||||||||
35397|Killi Killi Formation|61405|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group. Interbedded muscovite psammite and pelite, graded beds (not exposed).   Age: >1835Ma.  Geological Province: Arunta region - Aileron Province.||||||07-NOV-08
35397|Killi Killi Formation|61861|3|Fully described|p12-14, p4, 9-10, 15, Figs.16-21,  Map 1|Orosirian|Orosirian|Most widespread formation in Tanami Group. Typically deeply weathered and outcrops poorly. Forms incomplete Bouma sequences. Thickness to 4 km. Intruded by basalt-dolerite sills and feldspar porphyry dykes. Age based on youngest detrital zircons and age of intruding granite|Between 1843 +/- 68 and 1840 +/- 11 Ma.|Youngest unit in Tanami Group.|Includes informal 'jasper chert member' near or at top.|Overlies Dead Bullock Formation, transitionally in places. Faulted against Twigg Formation: may be lateral equivalent. Unconformably overlain by Birrindudu Group, Pargee and Muriel Range Sandstones.|Thick sequence of turbiditic sandstone: micaceous greywacke, quartzwacke, lithic greywacke, quartz arenite and lithic arenite, interbedded with siltstone and mudstone and occasional thin chert beds.|03-APR-12
35397|Killi Killi Formation|62377|4|Described|p5, 21-29|Paleoproterozoic|Paleoproterozoic|Conformably overlies the Dead Bullock Formation. Turbiditic sediments. Correlated with Lander Rock beds and Olympio Formation. Unconformably overlain by the Pargee Sandstone and the Gardiner Sandstone. Age: 1840 +/- 18, 1828 +/- 32Ma.||||||07-NOV-08
35397|Killi Killi Formation|62580|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group. Thick sequence of turbiditic sedimentary sandstone and siltstone.||||||07-FEB-11
35397|Killi Killi Formation|62628|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group. Geological Province: Tanami Inlier. Greywacke, micaceous; quartzwacke, quartzarenite, siltstone, graphitic siltstone, granule conglomerate.||||||07-NOV-08
35397|Killi Killi Formation|62632|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group. Geological Province: Tanami/Arunta Region-Aileron Province. Interbedded low grade muscovite bearing psammite and pelite.||||||07-NOV-08
35397|Killi Killi Formation|62636|6|Mentioned|Map Legend|||Solid Geology legend.||Of Tanami Group.||||15-APR-11
35397|Killi Killi Formation|62637|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group. Geological Province: Tanami/Arunta Region - Aileron Province. Interbedded muscovite bearing psammite and pelite, graded beds.||||||07-NOV-08
35397|Killi Killi Formation|63261|3|Fully described|p9 Fig. 5, p11-12, p23|Paleoproterozoic|Paleoproterozoic|Of Tanami Gp.Conformable on Dead Bullock Fm. Age:<1840Ma.Thick succession of monotonous turbiditic rocks. Correlated with widespread Lander Rock beds in Arunta region. Geol.prov: Tanami Region.Former Madigan beds of Smith et al (1998), Detailed lithol.||||||07-FEB-11
35397|Killi Killi Formation|63866|5|Briefly described|p92-p93|||Tanami Region.||||Overlies the Dead Bullock Formation.|Sandstones.|
35397|Killi Killi Formation|64277|5|Briefly described|Map ledgend|Paleoproterozoic|Paleoproterozoic|Of Tanami Group. Age: c. 1835Ma. Feldspathic wacke, sandstone, siltstone, and mudstone, minor quartzite, banded chert, dolerite, and gabbro sills; metamorphosed.||||||24-JUN-08
35397|Killi Killi Formation|64662|5|Briefly described|p28, 27, p30 Fig. 3, p34-37, p43|Orosirian|Orosirian|Of Tanami Gp. Age: Constrained between conformably underlying 1838+/-6Ma Callie Member and intrusive 1.82Ga Water Tower Tonalite.Turbidite, including greywacke, qtz arenite + qtz wacke - youngest detrital zircons are ~1.86 Ma (See Tbs.1, 2).||||||07-FEB-11
35397|Killi Killi Formation|64675|5|Briefly described|p9, p10, p12, Fig.12, pp16-18, p23|Orosirian|Orosirian|Youngest detrital zircon age. See also Map 1.|1848 +/- 22 Ma (AGSO OZCHRON)|Of the Tanami Group.||Underlain by the Dead Bullock Formation. Overlain by the Twigg Formation. Unconformably overlain by the Pargee Sandstone.|Comprises a thick turbidite sequence of interbedded shale, siltstone, and medium-thick bedded sandstone.|19-MAR-14
35397|Killi Killi Formation|64722|5|Briefly described|p10|Orosirian|Orosirian|Detrital zircon population dominated by 1880 - 1840 Ma ages.||Of Tanami Group.||||11-APR-12
35397|Killi Killi Formation|64725|5|Briefly described|p63 Fig.7.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. See also reference to Killi Formation on p.62.|c.1840 Ma.|Upper unit in Tanami Group.||||03-APR-12
35397|Killi Killi Formation|64733|4|Described|p171-176, p182, Figs.2, 4, 6, 7|Orosirian|Orosirian|Up to 4km thick. Age from detrital zircon U-Pb SHRIMP (Cross and Crispe, 2007). Thought by Blake et al. (1979) and Tunks (1996) to be lateral equivalent of Mount Charles Formation. In faulted contact with Stubbins Formation in places.|Maximum depositional age 1864+/-4 Ma.|Of Tanami Group.||Overlies Dead Bullock and Stubbins Formations and Callie Member. Unconformably overlain by Ware Group.|Turbiditic sandstone, pelite and rare dolerite sills.|20-APR-12
35397|Killi Killi Formation|64734|4|Described|p186-189, p194-6, p199, p201-2, Fig.2|Orosirian||Sst, thinly bedded siltst; fine sand grading to clayst (some black); upper Tanami Group; laterally extensive; varying thickness; geochemical similarities to Upper Callie Sequence; conformable boundary with Dead Bullock Formation below suggested||||||10-MAR-10
35397|Killi Killi Formation|64735|5|Briefly described|p211, p217,||Orosirian|Correlated with Lander Package.||||Overlain by Ware Group.||30-APR-12
35397|Killi Killi Formation|64737|5|Briefly described|p233, p234 Fig.4, p236 Tab.4, p241||Orosirian|Dominated by ~1840-1880 Ma detrital zircons. Similar provenance and depositional timing to Lander Package and Ooradidgee Group. Age is a maximum depositional age.|1868-1866 Ma.|Of Tanami Group.||Overlies Dead Bullock Formation.||01-MAY-12
35397|Killi Killi Formation|64956|5|Briefly described|p10|||Conformably overlain by the informally named "Sunset Pound sandstone".||||||07-FEB-11
35397|Killi Killi Formation|65323|5|Briefly described|Map legend|Orosirian|Orosirian|Sandstone, siltstone; non to weakly magnetic; includes the informal Jasperlitic Chert member; of the Tanami Group; overlies Dead Bullock Formation||||||02-FEB-10
35397|Killi Killi Formation|65324|5|Briefly described|Map legend|Orosirian|Orosirian|Of Tanami Group; includes informal Jasperlitic Chert member; overlies Dead Bullock Formation. Purple, brown, turbiditic, bedded, micaceous, silty-quartzitic sst interbedded with buff-dark grey siltst with minor pebbly sst, chert; volcanic lithics in west||||||
35397|Killi Killi Formation|65326|5|Briefly described|Map legend|Orosirian|Orosirian|Sandstone, siltstone; non to weakly magnetic; includes the informal Jasperlitic Chert member; of the Tanami Group; overlies Dead Bullock Formation||||||02-FEB-10
35397|Killi Killi Formation|65327|5|Briefly described|Map legend|Orosirian|Orosirian|Sandstone, siltstone; non to weakly magnetic; includes the informal Jasperlitic Chert member; of the Tanami Group; overlies Dead Bullock Formation||||||
35397|Killi Killi Formation|65328|5|Briefly described|Map legend|Orosirian|Orosirian|Sandstone, siltstone; non to weakly magnetic; includes the informal Jasperlitic Chert member; of the Tanami Group; overlies Dead Bullock Formation||||||02-FEB-10
35397|Killi Killi Formation|65335|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tanami Group. Interbedded muscovite psammite and pelite, graded beds.||||||
35397|Killi Killi Formation|65338|5|Briefly described|p17.|||Tanami Region. Overlies a tuff dated at 1838 +/- 5 Ma (Cross and Crispe 2007). Detrital zircon data is remarkably consistent with that from Lander Rock Formation, with which it is correlated.||||||
35397|Killi Killi Formation|65349|5|Briefly described|Map legend|Orosirian|Orosirian|Of Tanami Group; overlies Dead Bullock Formation; includes informal Jasperlitic Chert member. Purple, brown, turbiditic, bedded, micaceous, silty-quartzitic sst interbedded with buff-dark grey siltst, minor pebbly sst, chert; volcanic lithics in west ||||||
35397|Killi Killi Formation|65350|5|Briefly described|Map legend|Orosirian|Orosirian|Of Tanami Group; includes informal Jasperlitic Chert member; overlies Dead Bullock Formation. Purple, brown, turbiditic, bedded, micaceous, silty-quartzitic sst interbedded with buff-dark grey siltst with minor pebbly sst, chert; volcanic lithics in west||||||02-MAR-10
35397|Killi Killi Formation|65351|5|Briefly described|Map legend|Orosirian|Orosirian|Of Tanami Group; includes informal Jasperlitic Chert member; overlies Dead Bullock Formation. Purple, brown, turbiditic, bedded, micaceous, silty-quartzitic sst interbedded with buff-dark grey siltst with minor pebbly sst, chert; volcanic lithics in west||||||
35397|Killi Killi Formation|65352|5|Briefly described|Map legend|Orosirian|Orosirian|Sandstone, siltstone; non to weakly magnetic; includes the informal Jasperlitic Chert member (not shown on map); of the Tanami Group; overlies Dead Bullock Formation||||||02-FEB-10
35397|Killi Killi Formation|65353|5|Briefly described|Map legend|Orosirian|Orosirian|Sandstone, siltstone; non to weakly magnetic; includes the informal Jasperlitic Chert member (not shown on map); of the Tanami Group; overlies Dead Bullock Formation||||||02-FEB-10
35397|Killi Killi Formation|65354|5|Briefly described|Map legend|Orosirian|Orosirian|Sandstone, siltstone; non to weakly magnetic; includes the informal Jasperlitic Chert member; of the Tanami Group; overlies Dead Bullock Formation||||||
35397|Killi Killi Formation|65355|5|Briefly described|Map legend|Orosirian|Orosirian|Sandstone, siltstone; non to weakly magnetic; includes the informal Jasperlitic Chert member; of the Tanami Group; overlies Dead Bullock Formation||||||
35397|Killi Killi Formation|65356|5|Briefly described|Map legend|Orosirian|Orosirian|Sandstone, siltstone; non to weakly magnetic; includes the informal Jasperlitic Chert member (not shown on this map); of the Tanami Group; overlies Dead Bullock Formation||||||02-FEB-10
35397|Killi Killi Formation|65358|5|Briefly described|p6|||In Tanami Region. Conformably overlies Dead Bullock Formation. Turbiditic succession. Correlated with Lander Rock Formation in the Arunta Region.||||||
35397|Killi Killi Formation|66129|5|Briefly described|p213, p214 Fig.1, p215 Fig.2, p216 Fig.3|Orosirian|Orosirian|1864-1844 Ma. Turbiditic sandstone, siltstone, shale. Conformably overlies Stubbins and Dead Bullock Formations. Contact metamorphosed. Unit in Tanami Group. Contains Bald Hill Member.||||||
35397|Killi Killi Formation|66468|5|Briefly described|p16-17,p19-20, p21 Fig.6, p22-24, p26-27|Orosirian|Orosirian|1864-1844 Ma. Conformably overlies Stubbins Formation (WA) and Dead Bullock Formation (NT). ~5km thick, medium to coarse grain sandstone that grades into finer-grain sandstone, laminated siltstone and shale succeeded by mudstone and rare dolerite sills.||||||
35397|Killi Killi Formation|67127|6|Mentioned|p111, p168|||Associated with uraniferous xentime and xenotime rich in HREE and a U-REE mineralisation between the unconformity of this unit and the overlying Gardiner Sandstone.||||Unconformably underlies the Gardiner Sandstone.||
35397|Killi Killi Formation|67163|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.||Unit in Tanami Group.||Overlies Dead Bullock Formation.|Interbedded low-grade muscovite-bearing psammite and pelite, graded beds.|20-OCT-11
35397|Killi Killi Formation|67165|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province. Low to medium gravity response.||Unit in Tanami Group.||Overlies Dead Bullock Formation.|Interbedded muscovite-bearing psammite and pelite, graded beds.|20-OCT-11
35397|Killi Killi Formation|67168|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lateral equivalent of upper part of Twigg Formation. Includes a jasperlitic chert unit.||Unit in Tanami Group.||Overlies Dead Bullock Formation. Is unconformably overlain by Pargee Sandstone and by Gardiner Sandstone.|Sandstone, siltstone, jasperlitic chert.|
35397|Killi Killi Formation|67352|6|Mentioned|p50|||||||||
35397|Killi Killi Formation|67824|4|Described|p383, p386-p396|Orosirian|Orosirian|Hosts gold. Prospectivity increases where crustal-penetrating structures intersect claystone facies. Maximum age constrained by the underlying Callie Member. Deepwater below wave base setting. Sedimentary units were sourced from NW. Also aged 1864-1844 Ma.|< 1840 Ma|Of the Tanami Group.||Overlies Callie Member (Dead Bullock Formation). Conformably overlies Stubbins Formation. Is overlain by Tanami Group.|Mainly turbidites: fine-grained, micaceous-lithic muddy sandstone interbedded with siltstone and claystone.|
35397|Killi Killi Formation|67826|4|Described|p401 Fig.2, p402, p402 Fig.3, p404 Fig.4|Orosirian|Orosirian||~ 1864-1844 Ma|Of the Tanami Group.||Overlies  Stubbins Formation; layer-parallel fault contact. Conformably overlies Dead Bullock Formation.|Comprises metamorphosed wacke, siltstone, shale.|
35397|Killi Killi Formation|68474|5|Briefly described|p572-574, p585|||Granites-Tanami Orogen. 5km thick.|ca. 1864-1844 Ma|Tanami Group||Conformably overlies the Stubbins Formation, Mount Charles Formation and the Dead Bullock Formation. Unconformably overlain by the Ware Group.|Turbiditic succession.|
35397|Killi Killi Formation|68656|4|Described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleoproterozoic|Paleoproterozoic|Tanami Basin. See also 100k_maginterpgeop_lut.csv, and GEOCHRON. Granites-Tanami Complex. Moderate gravity, non-magnetic. Contains detrital zircons with a wide range of ages, discussed in the GEOCHRON folder.|1862 +/- 3 Ma (Wingate et al., 2009).|Unit in Tanami Group.||Conformably overlies Dead Bullock Formation. Correlated with Lander Rock Formation. Is intruded by Balwina Granite. Is overlain unconformably by Ware Group.|Feldspathic metawacke, metasandstone, metasiltstone and metamudstone; minor quartzite, banded metachert, metabasalt, metadolerite, metagabbro|
35397|Killi Killi Formation|68733|6|Mentioned|p184|Paleoproterozoic|Paleoproterozoic|Tanami Region.||||||05-DEC-17
35397|Killi Killi Formation|68994|5|Briefly described|p6|||||Tanami Group||Is equivalent to Lander Rock Formation.||
35397|Killi Killi Formation|69003|5|Briefly described|p16-17|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. Up to 5km thick. The age of the occurrence in NT is shown as <1840 Ma.|1864-1844 Ma.|Tanami Group.||Unconformably overlies the Stubbins, Mount Charles and Dead Bullock Formations. Is overlain unconformably by the Ware Group.|Turbiditic sandstones, siltstones and shales.|
35397|Killi Killi Formation|69253|4|Described|p746, p747 Fig.1, p748, p755-767|Orosirian|Orosirian|Maximum depositional age of c.1864 Ma (SHRIMP U-Pb zircon; Bagas et al., 2009). ~5 km thick. Petrophysical properties detailed. Hosts gold mineralisation in the Coyote area.|~1864-1844 Ma.|Unit in Tanami Group.||Conformably overlies Dead Bullock Formation. Is intruded by Selby Granite.|Upward-fining succession of turbiditic sandstone that grades upwards into siltstone and mudstone.|
35397|Killi Killi Formation|69288|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.||Tanami Group.|||Interbedded low-grade muscovite-bearing psammite and pelite; graded beds.|
35397|Killi Killi Formation|69383|6|Mentioned|p70|||Tanami Region. Detrital zircon spectra compared to Utopia Quartzite spectra.||||||
35397|Killi Killi Formation|69417|5|Briefly described|p2:4,|||Tanami Region. Turbiditic succession.|1845-1835 Ma.|||||12-JUL-16
35397|Killi Killi Formation|69418|6|Mentioned|p3:7|||Tanami Region. Hosts gold deposits (described).||||||12-JUL-16
35397|Killi Killi Formation|69424|6|Mentioned|p9:4|Paleoproterozoic|Paleoproterozoic|Tanami Region.||||Correlative of Ooradidgee Group.||12-JUL-16
35397|Killi Killi Formation|69426|4|Described|p11:3-8, 10-11, 14, 26, 30-31, 36|Orosirian|Orosirian|Thickness <4000m. Turbiditic, deep-marine proximal to mid-fan setting. Metamorphosed to greenschist to middle amphibolite facies. Hosts gold mineralisation at the Tregony and Titania prospects, and The Don U-Au occurrence. Is intruded by a tonalite aged 1821 +/- 4 Ma. Is separated from the Century Formation by the Pargee Fault.||Tanami Group.||Transitionally overlies Dead Bullock Formation. Is overlain unconformably by Ware Group, Mount Charles and Killi Killi Formations and Pargee Sandstone. Correlated with Lander Rock Formation.|A thick succession of micaceous greywacke, quartz greywacke, lithic greywacke, quartz sandstone and lithic sandstone, interbedded with siltstone (in part carbonaceous) and mudstone, and occasional thin chert beds.|12-JUL-16
35397|Killi Killi Formation|69427|5|Briefly described|p12:4-6|||Tanami Region. Age of a tuff immediately underlying this Formation.|<1838 +/- 5 Ma (Cross and Crispe, 2007).|||Stratigraphic equivalent of Lander Rock Formation.||12-JUL-16
35397|Killi Killi Formation|69587|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Geological province: Granites-Tanami Orogen, North Australian Craton. Of Tanami Basin. Events: Alice Springs Orogeny; Tanami Orogeny D1t. Sample GSWA 177278 (metagreywacke) yielded a concordant age of 1844+\-36 Ma, interpreted as maximum depositional age for the greywacke. Sample GSWA 178803 (sandstone) yielded a weighted mean 207Pb*/206Pb* date of 1862+\-3 Ma,  interpreted as maximum depositional age of the sandstone. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|1840-1835 Ma (inferred)|Unit of Tanami Group.||Overlain by Dead Bullock Formation. Intruded by Balwina Granite.|Feldspathic metawacke, metasandstone, metasiltstone, and metamudstone; minor quartzite, banded metachert, metabasalt, metadolerite, and metagabbro|
35397|Killi Killi Formation|69618|4|Described|p89-99, p100 Tb.1, p102, p104, p106-110|Paleoproterozoic|Paleoproterozoic|Hosts the Coyote gold deposit. Sandier and more typical of turbidites than shale-rich Dead Bullock (and Stubbins) Formations. Thickness estimated c.4km. Boundary with Dead Bullock Formation revised upwards to move Madigan beds, Stubbins and Mount Charles Formations into the underlying Callie Member of the Dead Bullock Formation.|~1864-1844 Ma.|Unit in Tanami Group.||Conformably overlies Dead Bullock Formation.|Siliciclastic units: typically fine-grained interbedded shale-topped sandstones.|30-MAR-15
35397|Killi Killi Formation|69747|4|Described|p262,264-265|Orosirian|Orosirian|Geological province: Tanami Block, North Australian Craton. Deposited in an active continental margin from a provenance predominantly containing Meso- to Neoarchaean granitic and minor mafic volcanic rocks near its base.|ca. 1864-1844 Ma|Unit of Tanami Group.||Upper unit of the Tanami Group. Underlain conformably by Dead Bullock Formation.|Fine- to coarse-grained, poorly sorted immature sandstone units that commonly grade upwards into siltstone and mudstone.|
35397|Killi Killi Formation|69917|6|Mentioned|p87|||Tanami Region. One of a number of North Australian Craton sources of zircons older than 1900 Ma. ||||||
35397|Killi Killi Formation|70024|6|Mentioned|p35|||||Tanami Group.||Conformably overlies Dead Bullock Formation.||
35397|Killi Killi Formation|70130|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.||Tanami Group.|||Contact-metamorphosed feldspathic metawacke, metasandstone, metasiltstone, and metamudstone; biotite zone.|
35397|Killi Killi Formation|70141|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.||Tanami Group.||Overlies Stubbins Formation. Is overlain by Gardiner Sandstone.|Contact-metamorphosed feldspathic metawacke, metasandstone, metasiltstone and metamudstone; biotite zone.|
35397|Killi Killi Formation|70142|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.||Tanami Group.||Is faulted against Slatey Creek Granite.|Biotite-zone contact metamorphosed feldspathic metawacke, metasandstone, metasiltstone and metamudstone.|
35397|Killi Killi Formation|70143|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. The contact metamorphosed areas of this Formation are mapped separately.||Tanami Group.|||Feldspathic metawacke, metasandstone, metasiltstone and metamudstone; minor quartzite, banded metachert, metabasalt, metadolerite and metagabbro. Locally contact metamorphosed to biotite zone.|
35397|Killi Killi Formation|70154|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic||1835-1840 Ma||||Feldspathic metawacke, metasandstone, metasiltstone, metamudstone, metadolerite and metagabbro, minor quartzite, banded metachert, and metabasalt|
35397|Killi Killi Formation|70291|4|Described|p178-179,181,183,185-189,191,199,201-202|Paleoproterozoic|Paleoproterozoic|Geological province: Tanami. Provenance is likely from Kimberly region to the west. Maximum depositional age 1840 Ma. Intruded by foliated dolerite sills.|<1840 Ma|Unit of Tanami Group.||Upper unit of Tanami Group. Underlain by Dead Bullock Formation.|Coarse-grained turbiditic sandstone and silstone.|
35397|Killi Killi Formation|70478|5|Briefly described|p2 Fig 1, 3-4|Statherian|Paleoproterozoic|Geological Province: Tanami. Minimum, post-deformation age from Frederick Suite granodiorite intrusions at 1802+/-4 Ma, 1801+/-4 Ma.||Unit of Tanami Group||Intruded by Frederick Suite granite.||
35397|Killi Killi Formation|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.||Tanami Group.||Overlies Callie Member (Dead Bullock Formation).|Micaceous greywacke, quartz greywacke, lithic greywacke, quartz sandstone, siltstone, graphitic siltstone, interbedded muscovite-bearing psammite and pelite, graded beds.|
35397|Killi Killi Formation|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.||Tanami Group.||Overlies Dead Bullock Formation.||
35397|Killi Killi Formation|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Of Tanami Basin. Events: Alice Springs Orogeny (450-295 Ma); Stafford Event (1810-1790 Ma); Tanami Event (1850-1830 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|1864-1830 Ma (inferred)|Unit of Tanami Group.|||Schistose to phyllitic greywacke, siltstone and shale; minor lithic sandstone, granule conglomerate, quartzite, banded chert, basalt and dolerite.|
35397|Killi Killi Formation|71302|5|Briefly described|p73|Paleoproterozoic|Paleoproterozoic|Geological province: Tanami region. Paleoproterozoic metasedimentary sequence exposed on the North Australian Craton, and possibly one of several sources of zircon provenance to the Inverway Metamorphics.||||||
35397|Killi Killi Formation|71348|6|Mentioned|p209,214-215|||Geological province: Tanami Region, North Australian Craton. See p215 for summary of U-Pb geochronological data.||||||
35397|Killi Killi Formation|71349|5|Briefly described|p724-725, p737|Paleoproterozoic|Paleoproterozoic|Tanami Region. Contains zircons aged c.3.1 Ga (significance explained).|1840 Ma.|Tanami Group.||Overlies Dead Bullock Formation.|Turbidites.|
35397|Killi Killi Formation|71397|4|Described|p1,5,22,46-48|Orosirian|Orosirian|Geological province: Granites-Tanami Orogen. Deposited as part of a basin-floor fan system (Lamback et al., 2012). May have been formed at an active margin, possibly contiguous with Kimberley margin (Hollis et al., 2010; Hollis and Glass, 2012). Timing of deposition is constrained to after c. 1864 Ma (age of underlying Stubbins Formation), and before the 1840-1825 Ma Tanami Orogeny (Vandenberg et al., 2001). Contain detrital zircons with dominant age components at 1870-1860 Ma and at c. 2500 Ma; similar to that of Olympio Formation. Geochemical analysis suggest a similar sedimentary and chemical source to the Killi Killi and Olympio formations, and interpreted to have been derived from from granitic rocks of the Paperbark Supersuite in the Western Zone of the Lamboo Province (Hollis et al., 2014).|1864-1840 Ma|Unit of Tanami Group.|||Monotonous, variably micaceous and lithic, turbiditic metasandstone that are interbedded with metasiltstone.|
35397|Killi Killi Formation|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1840+/-10 Ma (MDA: U-Pb zircon SHRIMP)||||Quartz wacke, greywacke, quartz arenite.|
35397|Killi Killi Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Tanami Basin, Granites-Tanami Orogen.||Tanami Group|||Feldspathic metawacke, metasandstone, metasiltstone, metamudstone, metadolerite, and metagabbro; minor quartzite, banded metachert, and metabasalt.|
35397|Killi Killi Formation|72366|5|Briefly described|p2|Orosirian|Orosirian|Geological province: Tanami Province. Age constrained by an overlying tuff with 1838+\-5 Ma magmatic crystallisation age (Cross and Crispe 2007). ||||Correlable to Lander Rock Formation.||
35397|Killi Killi Formation|72527|6|Mentioned|p192.|Paleoproterozoic|Paleoproterozoic|Given as an example of a metasedimentary unit that has a similar detrital zircon spectra to Murphy Metamorphics. Ref Hollis et al., 2010; Carson, 2013; Cross and Crispe, 2007; Bodorkos et al., 2013; Kositcin et al., 2012, 2013, 2014, 2015a).||||||
35397|Killi Killi Formation|73089|4|Described|p: 3-8, 11, 13-16, 18, 20, 22-33, 41, 43|Orosirian|Orosirian|Granites-Tanami Orogen. Hosts some Au mineralisation. 4 km thick. Compositionally immature. Interpreted to have been deposited as part of an extensive turbidite system proximal to mid-fan. Relatively high proportion of sandy units deposited as channelized or sheet sand lobes. Geochron metasandstone sample numbers = GA2004085001 and GA 2001082009 [see report for geochon details]. Paleoproterozoic-dominated source terrain. Lithologically more homogeneous than the underlying Dead Bullock Formation.|1840-1820 Ma [1865-1840 Ma?].|Tanami Group||Transitionally underlain by Dead Bullock Formation. Unconformably overlain by Pargee Sandstone. Intruded by Lewis Granite. May correlate to Olympio Formation (Halls Creek Group).|Siliciclastic metasedimentary rocks including micaceous greywacke, quartz wacke, lithic greywacke, quartz and lithic arenite, siltstone and mudstone.|
35397|Killi Killi Formation|73158|4|Described|p2 Fig.1, p3, p9, p10 Fig.9|Orosirian|Orosirian|Granites-Tanami Orogen.|1868+/-7 Ma MDA|Tanami Group||Overlies Dead Bullock Formation|Greywacke deposited as turbidites with increasing thickness towards the west.|
35397|Killi Killi Formation|73159|5|Briefly described|p2 Fig.1, p3, 9, p10 Fig.9|Proterozoic|Proterozoic|Granites-Tanami Orogen. Sediments sourced from nearby continental margin. HFSE geochemical plots.|1866 +/- 7 Ma (MDA).|Tanami Group.||Overlies Dead Bullock Formation.|Felsic greywacke turbidites; thickness increases westwards.|
35397|Killi Killi Formation|73445|5|Briefly described|p7||||1864 +/- 6 Ma (MDA: Bagas et al., 2009).|||Is overlain unconformably by the Redcliff Pound Group.||
80176|Kilykilykarri Member|71211|4|Described|ii, ix, p21, p26, p27 fig 2.3, p28-p30|Neoproterozoic|Mesoproterozoic|Less than or equal to 50m thick. Deposited in a shallow water environment as a turbidite. See also p38, p54-p57, p59-p61, p63, p66, p68, p86, p87 fig 3.2, p100, p137-p139, p208, p266. ||Kathleen Ignimbrite||Overlies the Karlaya Member. Overlain by the Rowland Suite.|Well-sorted, stratified and graded, rhyolitic, volcaniclastic interbedded pebbly conglomerate, breccia, sandstone and mudstone.|03-JUL-20
40489|Kimberley Group, lower|24572|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Informal.  Age: c.1805Ma.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
40489|Kimberley Group, lower|70826|6|Mentioned|p5 tbl 2, p9|Paleoproterozoic|Paleoproterozoic|Kimberley Basin.||Kimberley Group||||
40489|Kimberley Group, lower|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Kimberley Basin.||Kimberley Group|Includes Carson Volcanics, King Leopold Sandstone.||Quartz sandstone and feldspathic sandstone; siltstone and mudstone; basalt; minor dolostone and conglomerate; includes King Leopold Sandstone and Carson Volcanics.|
40484|Kimberley Group, upper|24572|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Informal.  Age: <1805Ma.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
40484|Kimberley Group, upper|70826|6|Mentioned|p5 tbl 2, p9|Paleoproterozoic|Paleoproterozoic|Kimberley Basin.||Kimberley Group||||
40484|Kimberley Group, upper|72034|6|Mentioned|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Mentioned as parent unit. Age assumed from constituents. No other data. Informal subdivision of Kimberley Group.||Kimberley Group|Includes Yampi Formation, Pentecost Sandstone, Elgee Siltstone, Warton Sandstone.|||
68664|Kimmys Bore Monzogranite|63420|5|Briefly described|Map legend|Archean|Archean|Of Split Rock Supersuite. Geological Province: Pilbara Craton. Biotite monzogranite; homogeneous, equigranular to seriate.||||||07-NOV-08
68664|Kimmys Bore Monzogranite|63441|5|Briefly described|p12 tb. 2|Archean|Archean|Of Split Rock Supersuite. Geological province: Pilbara Craton.||||||07-FEB-11
68664|Kimmys Bore Monzogranite|68281|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.||Of the Split Rock Supersuite.|||Biotite monzogranite; homogeneous, equigranular to seriate.|23-SEP-13
68664|Kimmys Bore Monzogranite|68283|5|Briefly described|Map Legend|Archean|Archean|Pilbara Craton.||Of the Split Rock Supersuite.|||Biotite monzogranite; homogeneous, equigranular to seriate.|23-SEP-13
68664|Kimmys Bore Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Biotite monzogranite; homogeneous, equigranular to seriate.|
68664|Kimmys Bore Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; Split Rock Supersuite Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|2851-2831 Ma (inferred)|Unit of Split Rock Supersuite.|||Biotite monzogranite; homogeneous, equigranular to seriate|
68664|Kimmys Bore Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
68664|Kimmys Bore Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Biotite monzogranite; homogeneous, equigranular to seriate.|
30669|King Granodiorite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1860Ma. Geological province: Kimberley Province (West).||||||07-FEB-11
30669|King Granodiorite|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|Approx 1865 - 1850 Ma.||||||
30669|King Granodiorite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Paperbark Supersuite.||||||07-NOV-08
80078|Kingia Sandstone|69182|6|Mentioned|p71|Early Permian|Early Permian|Only appears on Ch2 p71 in the Hovea 4 strat column. High Cliff Sst underlies, Irwin River Coal Measures overlie, so age inferred.||||||22-SEP-17
80078|Kingia Sandstone|73513|4|Described|p29, p31-33, p35-38, p40-41|||Perth Basin. Informal name for genetically distinct upper interval in High Cliff Sandstone with different reservoir characteristics, correlated throughout northern part of the basin. Upper shoreface and beach conditions. Transitional with the overlying Irwin River Coal Measures, top is difficult to define. Misspelt as Kinga Sandstone p31? Kingia unit p31 Fig.4. Reservoir for the Waitsia Field. Misspelt as Kingia Formation p35 Fig.7.||High Cliff Sandstone||Overlies Bit Basher Shale, underlies Irwin River Coal Measures|Thick bedded quartzose sandstone, 25-50 m thick.|
29247|Kingswood Basalt Member|30562|4|Described|p40|||See also P37||||||
29247|Kingswood Basalt Member|43162|6|Mentioned|6|||||||||
31363|Kirgella Granitoid Gneiss|43593|6|Mentioned|p4|||||||||
73692|Kiwirrkurra Formation|64580|4|Described|map legend|Neoproterozoic|Paleoproterozoic|Red-weathering lithic sandstone, quartz sandstone and conglomerate.||||||15-DEC-08
73692|Kiwirrkurra Formation|68994|4|Described|p1, p6-11, p17-19, p23, p25, p27|Neoproterozoic|Neoproterozoic|Not clear if it forms basal unit, or is older than, Amadeus Basin. Sample analysed is coarse-grained, pebbly sandstone. Detrital zircon U-Pb ages listed. Conservative max depositional age is 1633+/-6 Ma, however depositional age could be considerably younger (Kirkland et al. 2009). Hf analyses detailed.|>840 Ma.|||Unconformably overlies Pollock Hills Formation. Unconformably overlain by Heavitree Quartzite (contact not exposed).|Lithic sandstone, quartz sandstone, and conglomerate.|13-JAN-17
73692|Kiwirrkurra Formation|69003|6|Mentioned|p5|||West Arunta Orogen and Amadeus Basin.||||||
73692|Kiwirrkurra Formation|69510|6|Mentioned|p10|||Basal (western) Amadeus Basin. Mentioned as having close similarities with the detrital zircon spectrum of an un-named hematite-bearing quartzite aged 1236 +/- 64 Ma.||||||
73692|Kiwirrkurra Formation|69606|5|Briefly described|p4 fig 2|Mesoproterozoic|Mesoproterozoic|Amadeus Basin.|||||Sandstone.|
73692|Kiwirrkurra Formation|70762|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|North Australian Craton.|||||Red-weathering lithic sandstone, quartz sandstone, and conglomerate.|
73692|Kiwirrkurra Formation|71592|5|Briefly described|Appendix A.|||Amadeus Basin.|1633+/-6 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
73692|Kiwirrkurra Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoproterozoic|Paleoproterozoic||Max age 1633+/-6 Ma, min ~1000 Ma.||||Red-weathering lithic sandstone, quartz sandstone, and conglomerate.|
83642|Knapp Head dolerite dyke|73480|5|Briefly described|p212, p213 Fig.7, p214-215|Stenian|Stenian|Over 15 m wide steeply dipping dyke, northwest-strike. Suggested to be related to Marnda Moorn large igneous province. See also Knapp Head dyke p201 Fig.1, Knapp Head dolerite p216. Hosted in granite.|1124+/-80 Ma apatite U-Pb crystallisation age||||Medium-grained dolerite dyke, metamorphosed to at least greenschist facies.|
80120|Knobbly Gabbro|71212|4|Described|intro p2, intro p3, p46, p58, p89|||Yilgarn Craton. One of 5 informal units that are together equivalent to the formal Bounty Igneous Complex. Up to 300m thick.||||Overlies the Songvang Formation. Overlain by the Bounty Igneous Complex.|Medium-grained and massive to locally moderately-foliated gabbro.|26-SEP-17
26270|Knox Siltstone Member|13194|4|Described|p391 Tb. 4-16|||Type Section: Elf Aquitaine drill hole WBS 5048 15o27'S 128o59'E (199-280.4m).  Correlated to 122-244m of type section of Burt Range Formation.||Burt Range Formation, at Sorby Hills||Overlies Sorby Dolomite Member (locally disconformably). Overlain by Gooseneck Member.|Dolomitic siltstone and dolomite; basal dolomitic breccia.|
26270|Knox Siltstone Member|40792|2|Defined|p177|early Tournaisian|early Tournaisian|Mention P177 as Knox Siltstone||||||
26270|Knox Siltstone Member|41864|5|Briefly described|p102|||||||||
26270|Knox Siltstone Member|45169|6|Mentioned|Fig.4|||||||||
26270|Knox Siltstone Member|64694|5|Briefly described|p235, p239, p247, p252-253, p254 Fig.12|Tournaisian|Tournaisian|A possibe source of the Turtle-Barnett oil.||Unit in Burt Range Formation.||Unconformably overlies Sorby Dolomite Member.||
79246|Kockatea Sequence|69297|6|Mentioned|p204, p205, p207|Lower Triassic|Permian|Perth Basin. Deposited in a marine environment. Is the primary source for oil and condensate accumulations from the Dongara area fields of the onshore Perth Basin. See also p209, p223, p225, p236, p237, p238.|||Includes the Hovea Member.|Overlies the Hovea Member. Unconformably overlies the Dongara Sequence. Overlain by the Woodada Sequence.||
79246|Kockatea Sequence|70097|5|Briefly described|p4|Early Triassic|Early Triassic|Transgression and a maximum flooding event.||||||
34484|Kodj Kodjin Sandstone|22769|5|Briefly described|Table1p759||Miocene|||||||
25975|Kojarena Sandstone|23279|6|Mentioned|p29|||||||||
25975|Kojarena Sandstone|23816|4|Described|p242, 245|Bajocian|Bajocian|Geological Province: Perth Basin. Uppermost unit of the Champion Bay Group. Underlying unit: Newmarracarra Limestone. Overlying unit: Yarragadee Formation. Max. thickness: 34 m.||||||
25975|Kojarena Sandstone|24020|5|Briefly described|p387|Bajocian|Bajocian|Geological Province: Perth Basin||||||16-MAR-05
25975|Kojarena Sandstone|31561|6|Mentioned|p22|||Section||||||
25975|Kojarena Sandstone|31706|6|Mentioned|p665|||Jurassic correlation chart||||||
25975|Kojarena Sandstone|31910|6|Mentioned|p22|||||||||
25975|Kojarena Sandstone|32648|6|Mentioned|p32|||M. Jur.||||||
25975|Kojarena Sandstone|32649|4|Described|p25|||See also Table  1||||||
25975|Kojarena Sandstone|33022|6|Mentioned|p265|||Palaeomagnetism. See also P259||||||
25975|Kojarena Sandstone|33166|6|Mentioned|p58|||Refers bivalve faunas||||||
25975|Kojarena Sandstone|34134|6|Mentioned|Cor.Chart|||Middle Jurassic||||||
25975|Kojarena Sandstone|35282|6|Mentioned|Fig.27|||||||||
25975|Kojarena Sandstone|36257|6|Mentioned|Table 2.1|||||||||
25975|Kojarena Sandstone|36293|2|Defined|p156|Bajocian|Bajocian|||||||
25975|Kojarena Sandstone|36890|3|Fully described|p245|||||||||
25975|Kojarena Sandstone|41284|4|Described|p91|||||||||
25975|Kojarena Sandstone|41484|4|Described|p91|||||||||
25975|Kojarena Sandstone|44144|4|Described|p505 Tb.4-21|Bajocian|Bajocian|Type Section: Bringo railway cutting, 28o44'54''S 114o50'54''E. 34m thick shallow marine deposits.||Champion Bay Group||Conformably overlain by Yarragadee Formation. Overlies Newmarracarra Limestone conformably.|Red-brown, medium- to coarse-grained ferruginous sandstone; claystone at base.|
25975|Kojarena Sandstone|61811|4|Described|pp29-31, p64.|Middle Jurassic|Middle Jurassic|Type section in rail cutting, c. 24 km east of Geraldton; further details in Appendix 1.||Uppermost unit in Champion Bay Group.||Conformably overlies Newmarracarra Limestone. Is overlain conformably by Yarragadee Formation.|Ferruginous, medium- to coarse-grained sandstone; local basal claystone.|
25975|Kojarena Sandstone|64635|5|Briefly described|p16 |Middle Jurassic|Middle Jurassic|||Of the Champion Bay Group.||||
73564|Kooallup Limestone|62020|5|Briefly described|p177-190|Pleistocene|Pleistocene|Yalgorup Plain, southern Perth Basin. Diverse fossil foraminifera assemblage (listed). Paleoecological interpretations discussed.|||||Weakly cemented limestone.|
73564|Kooallup Limestone|63454|2|Defined|p71 Tb. 2, p75-76|Late Pleistocene|Late Pleistocene|Includes Lakeside, Bellevue and Springhill Members. Max. thickness: 16m; 10m at type section. On the Yalgorup Plain. Calcarenitic aeolianite, and beach and marine calcarenites; shoaling and seagrass facies.||||||
73564|Kooallup Limestone|67135|5|Briefly described|p62, p63 Fig.85.|Pleistocene|Pleistocene|Occurs as a series of prominent ridges parallel to the coast.|||||Calcarenite.|
73564|Kooallup Limestone|73206|4|Described|p856-860, p862, p864-865|Pleistocene|Pleistocene|Of Semeniuk (1997). Yalgorup Plain; restricted to the southern part of the central Swan Coastal Plain. Distinct from Tamala Limestone. Overlain by Kooallupland [landform]. Wedge-shaped to lensoid in plan view, where the seaward-edge forms a series of cusps. Shoaling upwards sequence records seagrass bank to beach to eolian facies (same as Tims Thicket Limestone). Includes a number of important smaller-scale features [see article]. Highly productive warm-water accumulation (supported by modern foram analogues) at a mean sea level of 4-4.5m above present mean sea level. [Article includes detailed discussion on geoheritage significance].||||Unconformably underlain[?] by Myalup Sand.|Limestone and intercalated sediments. Shoaling sequence including a lower, rich biofacies of shelly/fossiliferous limestone sharply overlain by beach facies containing swash zone molluscs, and an upper eolian unit.|
22123|Koolbye Formation|23047|6|Mentioned|38|||Of the Turee Creek Group. Hamersley Province. Overlain by Kazput Formation, underlain by Kungarra Formation.||||||10-FEB-09
22123|Koolbye Formation|23280|5|Briefly described|p1085,Fig2p1086|||||||||
22123|Koolbye Formation|23890|5|Briefly described|p16|Paleoproterozoic|Paleoproterozoic|Of Turee Creek Group. Geological Province: Pilbara Craton.||||||07-NOV-08
22123|Koolbye Formation|24544|4|Described|p47 Fig.35|Paleoproterozoic|Paleoproterozoic|Conformably overlies Kungarra Formation. Conformably overlain by Kazput Formation. Of Turee Creek Group.  Geological Province: Ashburton Province.||||||07-NOV-08
22123|Koolbye Formation|24607|5|Briefly described|p969 Fig. 2|||Of the Turee Creek Group.||||||
22123|Koolbye Formation|43290|3|Fully described|p7|||Of Turee Creek Group. Type section location given.||||||23-MAR-09
22123|Koolbye Formation|60373|5|Briefly described|p145 Tb. 1|||Of Turee Creek Group. Overlian by Kazput Formation, underlain by Kungarra Formation.||||||
22123|Koolbye Formation|62129|3|Fully described|p11-12|Archaean|Archaean|Of Turee Creek Group. Overlies conformably Kungarra Formation, overlain confomably by Kazput Formation. Thickness: 130m. Geological Province: Hamersley Basin. Fine- to coarse-grained quatrz sandstone, and minor argillite and conglomerate.||||||06-FEB-17
22123|Koolbye Formation|62130|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Turee Creek Group. Geological Province: Hamersley Basin, Pilbara Craton. Fine- to coarse-grained metamorphosed quartzitic sandstone, minor pelite and metaconglomerate.||||||23-MAR-09
22123|Koolbye Formation|66574|5|Briefly described|p914 Fig.3|||Of Turee Creek Group. Underlies Kazput Formation, overlies Kungarra Formation. Fluvial to shallow marine conglomerate and sandstone.||||||
22123|Koolbye Formation|67130|5|Briefly described|p3 fig 2|||||Turee Creek Group||Overlies Kungarra Formation, overlain by Kazput Formation|Quartzarenite, siltstone and minor conglomerate|
22123|Koolbye Formation|67183|6|Mentioned|p645 Tb.1|Archean|Archean|Present in the Southern Pilbara.||Turee Creek Group||||
22123|Koolbye Formation|68035|5|Briefly described|p292, Fig 6|Paleoproterozoic|Paleoproterozoic|Turee Creek Basin.||||Overlies Kungarra Formation, Meteorite Bore Member. Overlain by Kazput Formation.|Quartzite.|
22123|Koolbye Formation|68280|5|Briefly described|p5|Paleoproterozoic|Paleoproterozoic|||Turee Creek Group||Overlain by Kazput Formation, overlies Kungarra Formation, Meteorite Bore Member|Quartzite.|
22123|Koolbye Formation|69003|5|Briefly described|p7-8|||Turee Creek Basin.||Turee Creek Group.||Overlies ?conformably the Kungarra Formation. Is overlain unconformably by Kazput Formation.|Fluvial to shallow-marine sandstones.|
22123|Koolbye Formation|69028|5|Briefly described|Map Legend|Rhyacian|Siderian|Turee Creek Basin. Mapped with Kazput and Kungarra Formations as a single unit.|2445-2210 Ma|Of the Turee Creek Group.|||Mudstone, silstone, sandstone, conglomerate, local stromatolitic dolomite and basalt; metamorphosed.|07-MAY-14
22123|Koolbye Formation|69565|6|Mentioned|p133 Fig.1|||Hamersley Province.||Turee Creek Group.||Overlies Kungarra Formation. Is overlain by Kazput Formation.||
22123|Koolbye Formation|69754|5|Briefly described|p314-p315, p317, p339|||Pilbara Craton. Coastal-fluvial deposits. Outcrops in the Hardey Syncline.||Turee Creek Group||Disconformably overlies the Kungarra Formation. Overlain by the Kazput Formation.|Shallow-water (beach, fluvial and aeolian) sandstones.|
22123|Koolbye Formation|70086|5|Briefly described|p195-196,202|Paleoproterozoic|Paleoproterozoic|Geological province: Pilbara Craton. Of the Hamersley Basin. Depositional environment: tidal flat, beach, and fluvial deposits.||Unit of Turee Creek Group.||Overlain by Kazput Formation. Underalin by Kungarra Formation.||
22123|Koolbye Formation|70795|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|West Australian Craton, Turee Creek Basin|2445-2208 Ma||||Fine to coarse grained quartzitic metasandstone; minor pelite and metaconglomerate.|
22123|Koolbye Formation|71042|5|Briefly described|p66 fig 2|Paleoproterozoic|Paleoproterozoic|||Turee Creek Group||||
22123|Koolbye Formation|71112|5|Briefly described|p69,71-73,77,80|||Geological province: Pilbara Craton. Equivalent to Quartzite 1 of Trendall 1979.||||Overlain (locally unconformably) by Kazput Formation.|Fluvial siliciclastic sandstones.|
22123|Koolbye Formation|71550|4|Described|p35-38,42,44-45|Siderian|Siderian|Geological province: Of Hamersley Basin. Depositional environment: fluvial and shallow marine. U-Pb zircon analysis of quartz-rich sandstone from this study yield maximum age of 2.34 Ga. Detrital provenance is likely from erosive products of underlyng Hamersley Province and Pilbara basement.||Unit of Turee Creek Group.||Overlain by Kazput Formation. Underlain by Kungarra Formation.|quartz-rich sandstones.|03-SEP-19
22123|Koolbye Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Turee Creek Basin.||Turee Creek Group|||Fine- to coarse-grained quartzitic sandstone; minor argillite and conglomerate.|
22123|Koolbye Formation|72570|5|Briefly described|p2|||Deposited in a coastal to fluvial environment.||Turee Creek Group||Overlies the Kungarra Formation. Overlain conformably by the Kazput Formation.|Dominated by medium- to fine-grained, quartz rich sandstone interbedded with fine-grained sandstone and siltstone.|
22123|Koolbye Formation|72712|3|Fully described|p1, p9, p17, p19-p23, p29, p44.|Siderian|Siderian|Shown as KF on p20 Fig.15f. Maximum estimated thickness of about 160 m, but is generally about 130 m thick. Defined by Thorne and Tyler (1996). Maximum depositional age of <2430 Ma from detrital zircons points to erosion of underlying Woongarra Rhyolite rather than expected depositional age c. 2.34 Ga. Interpreted as tidal flat deposits, and as a beach deposit with eolian reworking and the upper horizon as fluvial. See also p5, p7, p14, p35, p36, p42, p47, p49, p29 Fig.22, p36 Fig.25, p43.|< 2438 +/- 6 Ma MDA.|Turee Creek Group||Conformably to unconformably overlies Kungarra Formation and conformably overlain by Kazput Formation, and unconformably by Munder and Anthiby Formations. Intruded by dolerite sills.|Includes medium to fine-grained, quartz-rich sandstone horizons, each separated by fine-grained sandstone and siltstone.|14-JAN-21
22123|Koolbye Formation|73538|5|Briefly described|p2 Fig. 1B, p3-4|||||Turee Creek Group||Underlain by Kungarra Formation. Overlain by Kazput Formation.|Quartz-rich sandstones.|
25129|Koolera Member|40347|6|Mentioned|p22|||||||||
34416|Kooline group|22716|6|Mentioned|p234|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
34416|Kooline group|50226|6|Mentioned|p416|||Informal name.||||||
31878|Koolyu Granite|24197|5|Briefly described|p26, p102 Tb. 14.1|Neoproterozoic|Neoproterozoic|Of O'Callaghan's Supersuite. I-type (granodioritic) Minyari type granite. Age: ~625Ma. Geological province: Paterson Province.||||||27-SEP-12
31878|Koolyu Granite|50436|5|Briefly described|p1.3, 4.1, Table 1.1|Neoproterozoic|Neoproterozoic|Supersedes Minyari Gneiss.  Geological Province: Paterson Orogen. Of the Minyari Group (O'Callaghans Supersuite).|||||monzogranite to syenogranite|27-SEP-12
31878|Koolyu Granite|67202|5|Briefly described|p189|||A unit in the Minyari group of granites (a subdivision of the O'Callaghans Supersuite by Goellnicht et al., 1991); assigned to the O'Callaghans Suite by Wyborn (1997) and Budd et al. (2001).||O'Callaghans Suite.||||
25978|Koombana Beach Rock|40367|2|Defined|p81|Holocene|Holocene|Unconformable over Tamala Limestone and remnants of Leschenault Fm. Modern beach rock of sand and gravelly sand cemented by magnesian calcite in a shoaling sequence showing shallow subtidal sand laminites underlain by trough-bedded gravelly sand and sand||||||07-AUG-07
22127|Koondooloo Monzogranite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  Age: c. 1835-1805 Ma.||||||07-NOV-08
22127|Koondooloo Monzogranite|23751|4|Described|p18|||Massively foliated, porphyritic, medium- to coarse-grained monzogranite. Of Kevins Dam suite.||||||
22127|Koondooloo Monzogranite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs Supersuite. Age: 1825Ma. Geological province: Kimberley Province.||||||07-FEB-11
22127|Koondooloo Monzogranite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  In the Bow River batholith.  Age: 1835-1805Ma.||||||07-NOV-08
22127|Koondooloo Monzogranite|43854|5|Briefly described|Map Legend||Proterozoic|oO Sally Downs supersuite.||||||12-AUG-08
22127|Koondooloo Monzogranite|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
22127|Koondooloo Monzogranite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
22127|Koondooloo Monzogranite|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Kevins Dam Suite (Sally Downs Supersuite).||||||07-NOV-08
22127|Koondooloo Monzogranite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Kevins Dam Suite|||Medium- to coarse-grained biotite monzogranite; foliated in places.|31-JUL-15
22127|Koondooloo Monzogranite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Kevins Dam Suite|||Medium to coarse grained biotite monzogranite, foliated in places.|
22127|Koondooloo Monzogranite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2.|1827-1808 Ma (Inferred)|Unit of Kevins Dam Suite.|||Medium- to coarse-grained biotite monzogranite; foliated in places|
22127|Koondooloo Monzogranite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1808-1827 Ma|Kevins Dam Suite|||Medium- to coarse-grained biotite monzogranite; foliated in places|
22127|Koondooloo Monzogranite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1827-1808 Ma (inferred)|Unit of Kevins Dam Suite.|||Medium- to coarse-grained biotite monzogranite; foliated in places|
22127|Koondooloo Monzogranite|72437|5|Briefly described|p11, p105|||Four analyses are derived from O'Brien (1994).||Kevins Dam suite|||Porphyritic biotite monzogranite.|
34998|Koongaling Volcanic Member|23046|5|Briefly described|171|||||||||
34998|Koongaling Volcanic Member|23570|3|Fully described|p148|Archean|Archean|Of Hardey Formation. Replaces Koongaling Volcanics of Hickman (1978).  Correlated with Bamboo Creek Member (Hardey Fm.). Age: 2764+/-8Ma. Overlain by Warri Warri Mamber.   Geological Province: Pilbara Craton||||||07-NOV-08
34998|Koongaling Volcanic Member|23575|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group.||||||07-NOV-08
34998|Koongaling Volcanic Member|23583|5|Briefly described|Map Legend|Archean|Archean|Of Hardey Formation. Overlain by Bamboo Creek Member. Geological Province Hamersley Basin.||||||07-NOV-08
34998|Koongaling Volcanic Member|23585|4|Described|p13|Archean|Archean|Age: c.2764-2757 Ma (U-Pb zircon). Previously Koongaling Volcanics. See also page 15. Of Hardey Formation. Underlain by Gregory Granitic Complex.||||||07-NOV-08
34998|Koongaling Volcanic Member|23594|4|Described|p13|Archean|Archean|Age: 2764+/-8 Ma (U-Pb zircon). Of Hardey Formation. Overlain by Warri Warri Member. Underlain by Gregory Granitic Complex. Geol. prov: Hamersley Basin. Max thickness: 2000 m.||||||07-NOV-08
34998|Koongaling Volcanic Member|23745|4|Described|p11|Archean|Archean|See also page 7 Fig 5. Of Hardey Formation.||||||07-NOV-08
34998|Koongaling Volcanic Member|23746|4|Described|p14|Archean|Archean|Of Hardey Formation. Geological Province: Hamersley Basin.||||||07-NOV-08
34998|Koongaling Volcanic Member|24025|5|Briefly described|p13|Archean|Archean|Of Hardey Formation.  Geological Province: Hamersley Basin.||||||07-NOV-08
34998|Koongaling Volcanic Member|50544|4|Described|p47, p15 Tb. 1|Archean|Archean|Basal unit of the Hardey Formation.  Overlies, and is genetically related to, the Gregory Granitic Complex; overlain by Warroo Hill Member.  Age: c.2764-2657Ma (SHRIMP U-Pb zircon; Arndt et al, 1991; Nelson, 1996, 1999).  See also p42-43.||||||07-NOV-08
34998|Koongaling Volcanic Member|50555|5|Briefly described|Map legend|Archean|Archean|Of the Hardey Formation (Fortescue Group, Mount Bruce Supergroup) - in the Gregory Range area. Porphyritic and fine-grained felsic lavas; dacite, rhyodacite and rhyolite.  Age: c.2764Ma.  Geological Province: Hamersley Basin.||||||07-NOV-08
34998|Koongaling Volcanic Member|61259|5|Briefly described|p404 Fig. 1|Archean|Archean|Of the Hardey Formation. Age: 2764+/-8Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
34998|Koongaling Volcanic Member|63417|5|Briefly described|Map legend|Archean|Archean|Of the Hardey Formation (Fortescue Group, Mount Bruce Supergroup). Age: c.2752Ma. Geological Province: Fortescue Basin. Porphyritic and fine-grained dacite, rhyodacite, rhyolite lava.||||||07-NOV-08
34998|Koongaling Volcanic Member|65827|6|Mentioned|p32|Neoarchean|Neoarchean|2766-2757 Ma; coeval with Bamboo Creek Member. Comagmatic with Gregory Granitic Complex.||||||21-JAN-22
34998|Koongaling Volcanic Member|66217|5|Briefly described|p46.|||Fortescue Basin. Coeval with granites of Gregory Range Suite.||Unit in Hardey Formation.|||Felsic volcanic and volcaniclastic rocks.|
34998|Koongaling Volcanic Member|67202|5|Briefly described|p236|Archean|Archean|Potential source rock for uranium.||Hardey Formation|||Porphyritic and fine-grained felsic lavas: dacite, rhyodacite, rhyolite; quartz-feldspar-mica schist.|15-FEB-18
34998|Koongaling Volcanic Member|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Hardey Formation|||Porphoryritic and fine-grained dacite, rhyodacite, rhyolite lava. Metarhyolite, metadacite and quartz-feldspar-mica schist.|
34998|Koongaling Volcanic Member|69299|6|Mentioned|p15|||Age of Lyre Creek Member is assumed to be similar to felsic Bamboo Creek and Koongaling Volcanic Members (of Hardey Formation, northeast Pilbara sub-basin), dated at c. 2760 Ma (Pidgeon, 1984; Arndt et al., 1991).||||||
34998|Koongaling Volcanic Member|69590|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Of Northeast Pilbara Sub-basin; Marble Bar Sub-basin, Fortescue Basin. Events: Pilbara Craton breakup. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|2764 Ma (isotopic)|Unit of Hardey Formation.|||Porphoryritic and fine-grained dacite, rhyodacite, rhyolite lava, metarhyolite, metadacite, and quartz-feldspar-mica schist.|
31899|Koongie Park Suite|24197|5|Briefly described|p85|Paleoproterozoic|Paleoproterozoic|Alkaline granite suite. Intruded between 1865Ma and 1818Ma. Geological province: Kimberley Province.||||||07-FEB-11
31899|Koongie Park Suite|50437|5|Briefly described|p1.6, 5.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Age: 1840Ma. Geological Province: Kimberley Region. Used interchangeably with Koongie Park Formation.||||||09-DEC-08
31899|Koongie Park Suite|71267|6|Mentioned|1M_geologyp12_lut.csv|||||||||
67860|Koonong Member|24544|4|Described|p48|Paleoproterozoic|Paleoproterozoic|Thick felsic lapilli tuff layer. Of Capricorn Group. Age: 1804+/-7 Ma. Geological Province: Ashburton Province.||||||07-NOV-08
67860|Koonong Member|24607|5|Briefly described|p969, 968|||Part of Capricorn Group. Felsic lapilli tuff dated at 1804+/-7 Ma.||||||
67860|Koonong Member|63866|5|Briefly described|p154|Statherian|Orosirian|Age from Hall et al., 2001 was recalculated to 1806 +/- 7 Ma by Evans et al., 2003.|1804 +/- 7 Ma (Hall et al., 2001)|Bywash Formation||||
67860|Koonong Member|63869|4|Described|p7-8, Plate 1|Paleoproterozoic|Paleoproterozoic|Named after Koonong Pool on southeast CAPRICORN  sheet. SHRIMP U-Pb zircon age from a felsic volcanic unit. Up to 20 m thick.|1804 +/- 7 Ma (Hall et al., 2002).|Unit in Bywash Formation.|||Tabular beds of silicified, massive or parallel-planar stratified, felsic volcaniclastic sandstone and accretionary lapilli tuff.|06-MAR-18
67860|Koonong Member|69024|5|Briefly described|Map Legend|Orosirian|Orosirian|Blair Basin.|c. 1804 Ma (Hall et al., 2001)|Of the Bywash Formation.|||Thin- to thick-bedded, massive to planar laminated felsic volcaniclastic rock, and accretionary lapilli tuff.|05-MAY-14
67860|Koonong Member|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|||Bywash Formation|||Thin- to thick-bedded, massive to planar laminated felsic volcaniclastic rock, and accretionary lapilli tuff|
67860|Koonong Member|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv|1804-1738 Ma|Bywash Formation|||Thin- to thick-bedded, massive to planar laminated, felsic volcaniclastic rock; contains accretionary and armoured lapilli.|
33898|Koonoonooka monzogranite|22450|6|Mentioned|p21||Archean|Yilgarn Craton||||||07-NOV-08
33898|Koonoonooka monzogranite|23281|6|Mentioned|p5,7|||||||||
33898|Koonoonooka monzogranite|24135|6|Mentioned|p7 Fig. 3|||Informal name.||||||
23705|Kopke Sandstone|1943|1|Redefined|p388, p373, p375 Fig.3, p376 Fig 4|Devonian||Only known from subsurface. Hocking (1985) erected type section in Yaringa-1 at 326-855m. The basal 33m are here assigned to underlying new unit, Faure Formation. Max. thickness stated: 486m (possible error as section interval = 496m). Age: no older than Late Silurian.||||Conformably overlies Faure Formation. Is conformably overlain by Sweeney Mia Formation.|Red and brown micaceous sandstone with minor siltstone and shale. Bioturbation at top of section and cross-bedding present. Mostly fluvial deposit.|
23705|Kopke Sandstone|6943|5|Briefly described|p599, pp601-606. |Early Devonian|Early Devonian|Contains conodonts. Up to 415 m thick; thickens to the northwest.||||Overlies Faure Formation. Is overlain by Sweeney Mia Formation.|Sandstone; minor dolomite, siltstone.|
23705|Kopke Sandstone|6944|6|Mentioned|p571.|Early Devonian|Early Devonian|Southern Carnarvon Basin. Disconformably underlies Nannyarra Formation.||||||27-OCT-14
23705|Kopke Sandstone|12471|6|Mentioned|p475 Fig.2. |Early Devonian|Early Devonian|||||||
23705|Kopke Sandstone|12729|4|Described|p.11, 26, 28, 32 4; Fig. 3-4, 6-10, 22-4|Emsian|Lochkovian|The type section: 326-822 m in Yaringa 1. 415 m thick. Central and southern Gascoyne Platform. Early Devonian age indicated from Ozarkodina pandora (lower Pedavis pesavis Zone). Prominent marker bed with high gamma is present near unit top. Deposition: deltaic > fluvial; stacking contrasting facies.||||Conformably overlies Faure Formation, conformably underlies Sweeney Mia Formation.|Upward-coarsening sandstone with minor dolomite and siltstone.|
23705|Kopke Sandstone|12731|5|Briefly described|p590 Fig.2.|Early Devonian|Early Devonian|Potential hydrocarbon reservoir.||||Overlies Faure Formation. Is overlain by Sweeney Mia Formation.|Sandstone, minor dolomite.|
23705|Kopke Sandstone|12733|5|Briefly described|p554 Fig.2.|Early Devonian|Early Devonian|Lochkovian-Pragian.||||Overlies Faure Formation. Is overlain by Sweeney Mia Formation.|Coarse-grained siliciclastics.|
23705|Kopke Sandstone|14227|5|Briefly described|Enclos. 2|||Presented as Kopke only - Sandstone inferred.||||||07-FEB-11
23705|Kopke Sandstone|14228|5|Briefly described|p5 fig2, p6 fig3, p7, p18, p26|Pragian|Lochkovian|Thickness to 496 m. Good reservoir characteristics; excellent aquifer.||||Overlies Faure Formation conformably. Overlain by Sweeney Mia Formation (conformably).|Upward coarsening redbed unit with minor dolomite and siltstone near the base.|
23705|Kopke Sandstone|23520|5|Briefly described|p18|Early Devonian|Early Devonian|||||||
23705|Kopke Sandstone|23572|4|Described|p8 Fig. 6, p10|Emsian|Lochkovian|Geological Province: Carnarvon Basin. Underlying Unit: Faure Formation (conformable). Overlying Unit: Sweeney Mia Formation (conformable). Max. thickness: <500m.||||||
23705|Kopke Sandstone|23726|5|Briefly described|p13|||Overlying unit Sweeny Mia Formation. Underlying unit Faure Formation. Geological Province: Carnarvon Basin.||||||
23705|Kopke Sandstone|23935|4|Described|p11 Fig.7|Emsian|Lochkovian|Conformably overlies Faure Formation. Conformably overlain by Sweeney Mia Formation. Geological Province: Southern Carnarvon Basin.||||||27-JAN-05
23705|Kopke Sandstone|24390|5|Briefly described|p19 Fig. 10|Devonian|Devonian|Geological Province: Southern Carnarvon Basin.||||||
23705|Kopke Sandstone|40617|2|Defined|p2|Late Silurian|Late Silurian|||||||
23705|Kopke Sandstone|41271|3|Fully described|p40|||Previously referred to as "Unknown formation, Unit B"||||||
23705|Kopke Sandstone|41438|6|Mentioned|p98|||See also Fig.5||||||
23705|Kopke Sandstone|42116|4|Described|p9|||See also Fig.1||||||
23705|Kopke Sandstone|42441|4|Described|Fig.2 P3|||See also P87.||||||
23705|Kopke Sandstone|49942|4|Described|p4 Fig.3, p9|Early Devonian|Early Devonian|Conformably overlies Faure Formation. Conformably overlain by Sweeney Mia Formation. Thickness: 496 m. Upward coarsening sandstone, with minor dolomite and siltstone. Deposited in a deltaic to fluvial environment. Geological Province: Gascoyne Platform.||||||
23705|Kopke Sandstone|50084|5|Briefly described|p77|Middle Devonian|Early Devonian|Grey to red, fine- to medium-grained sandstone. Conformably overlies Faure Formation. Geological Province: Southern Carnarvon Basin.||||||07-FEB-11
23705|Kopke Sandstone|50085|5|Briefly described|p19 Fig. 10|Devonian|Devonian|Geological Province: Southern Carnarvon Basin.||||||
23705|Kopke Sandstone|60384|5|Briefly described|p244, p243 Fig 2a|Early Devonian|Early Devonian|Southern Carnarvon Basin.||||Conformably underlain by Faure Formation. Overlain by Sweeney Mia Formation.|Upward-coarsening sandstone with minor dolomite and siltstone|
23705|Kopke Sandstone|60725|5|Briefly described|p29, p33 Fig.4, p35 Fig.5, p36 Fig.6. |Early Devonian|Early Devonian|||||Overlies Faure Formation.|Coarse-grained siliciclastics.|10-MAY-17
23705|Kopke Sandstone|61023|5|Briefly described|p34 Fig. 14|Devonian|Devonian|Geological Province: Southern Carnarvon Basin.||||||11-APR-08
23705|Kopke Sandstone|61562|5|Briefly described|p548 Fig. 3|Devonian|Devonian|||||||
23705|Kopke Sandstone|61563|5|Briefly described|p578 Fig. 2|Devonian|Devonian|See also p579 Fig. 3.||||||15-DEC-05
23705|Kopke Sandstone|64635|5|Briefly described|p6 ||||||||Sandstone, minor dolomite.|
23705|Kopke Sandstone|64972|6|Mentioned|p614, p617 Fig. 5|Early Devonian|Ealry Devonian|||||||
23705|Kopke Sandstone|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes grey - light brown sandstone finely laminated; red bed sandstone finely laminated; red/green/grey mottled siltstone/claystone.|
23705|Kopke Sandstone|67200|5|Briefly described|p7 fig 5|Devonian|Devonian|Thermal conductivity of 2.99 W/mK. See also p18 table 1, p46, p51, p56, app 2 tbl 1 p4. ||Kalbarri Group||Overlies Faure Formation, overlain by Sweeney Mia Formation|Sandstone with trough and parallel cross bedding. Finely laminated sandstone, mottled siltstone and claystone.|
23705|Kopke Sandstone|69029|6|Mentioned|p326,328|Pragian|Lochkovian|Of onshore Carnarvon Basin.||||Overlain by Sweeney Mia Formation. Underlain by Faure Formation.||
23705|Kopke Sandstone|69182|5|Briefly described|Ch3 p8, Ch3 p10-p11|Early Devonian|Early Devonian|Carnarvon Basin. Deposited in a fluvial or deltaic environment. See also Ch3 p23, Ch3 p30, Ch3 p67-p68, Ch3 p73.||||Conformably overlies the Faure Formation. Conformably overlain by the Sweeney Mia Formation.|Upwards-coarsening red-bed unit with minor dolomite and siltstone beds near the base.|
23705|Kopke Sandstone|69297|5|Briefly described|p246, p249|Early Devonian|Early Devonian|Gascoyne Sub-basin of the Carnarvon Basin. Deposited in a shallow marine environment. ||||Overlies the Faure Formation. Overlain by the Sweeney Mia Formation.|Mixed siliciclastics and dolomite.|
23705|Kopke Sandstone|69558|6|Mentioned|p95|Early Devonian|Silurian|Known from drilling in the area.||||||24-MAY-21
23705|Kopke Sandstone|69583|6|Mentioned|p134 Fig.3, p135, Plate 4|Early Devonian|Early Devonian|Seismic interpretation.||||||
23705|Kopke Sandstone|71146|5|Briefly described|p6|Pragian|Lochkovian|Southern Carnarvon Basin.||||Overlies the Faure Formation. Overlain by the Sweeny Mia Formation.|Sandstone.|
74422|Korojon-Miria group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||chalk, calcarenite, calcilutite, marl|
74110|Krackatinny Suite|24197|5|Briefly described|p21|Mesoproterozoic|Mesoproterozoic|Example of the Sally Downs Association. Emplaced at ~1310Ma(?). In the Paterson Orogen. Appears to intrude the Rudall Complex.||||||07-FEB-11
74110|Krackatinny Suite|68981|5|Briefly described|p4|||Tabletop Terrane, Rudall Province. Some felsic intrusive rocks have been dated at 1476 +/- 10 Ma and 1310 +/- 4 Ma.|c.1590-c.1550 Ma.||||Weakly deformed and metamorphosed felsic and mafic igneous rocks; minor quartzite, mafic and ultramafic schists, amphibolite, and banded iron-formation.|
74110|Krackatinny Suite|73168|5|Briefly described|p746-747, p762-763|early Mesoproterozoic|early Mesoproterozoic|Rudall Province. Tabletop Domain. Described rocks of variably deformed to undeformed leucogranites, hornblende-biotite-bearing granitoids, minor quartzo-feldspathic schist and amphibolite dykes appear to be correlated with the Krackatinny Suite of Maidment (2017). Associated with contact metamorphism, proposed to assign D2 regional foliations, folding and shear zone development to ca 1600-1550 Ma event and be referred to as the Krackatinny Event.|ca 1590-1550 Ma||||Intrusive rocks. Low and variable grade of deformation.|
31857|Krackatinny Supersuite|24197|5|Briefly described|p100|Mesoproterozoic|Mesoproterozoic|Includes Krackatinny and Kutakuta Tonalites, Harbutt Leucogranite and Runton Adamellite. Age: ~1310Ma (?). Geological province: Paterson Orogen.||||||07-FEB-11
31857|Krackatinny Supersuite|50436|5|Briefly described|p1.3, 3.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Age: 1310-1490Ma. Intrudes the Rudall Complex.||||||
31857|Krackatinny Supersuite|63866|5|Briefly described|p142-p143, p145, p148|||Tabletop Terrane, Rudall Complex.|c. 1600-1550 Ma|||||
31857|Krackatinny Supersuite|65454|5|Briefly described|p6|Calymmian|Calymmian|Tabletop Terrane. Many felsic and mafic intrusives. Emplaced during c.1590-1550 Ma, but youngest date obtained for felsic intrusives in the Terrane is 1310+/-4 Ma.||||||21-APR-16
31857|Krackatinny Supersuite|68100|6|Mentioned|p34|Mesoproterozoic|Mesoproterozoic|Tabletop terrane, Rudall Province|1600-1550 Ma|||||
31857|Krackatinny Supersuite|69003|5|Briefly described|p4, p40|Mesoproterozoic|Mesoproterozoic|Tabletop Terrane, Paterson Orogen.|1590-1550 Ma.||||Weakly deformed and metamorphosed felsic and mafic igneous rocks.|
31857|Krackatinny Supersuite|70084|6|Mentioned|p220|Calymmian|Calymmian|Geological province: Musgrave Province, Paterson Orogen. Correlable with Warlawurru Supersuite in the western Musgrave Province.||||||
31857|Krackatinny Supersuite|71169|5|Briefly described|iv-vi, p1, p7, p10-p11, p42, p52|||Tabletop Terrane, West Australian Craton. Previously defined to incorporate all the later stage felsic intrusive rocks exposed in the tabletop terrane, however dating from this study shows that the 1589-1549 rocks are distinct from the c. 1476 and 1286 Ma granites which thus defined as separate suites. See also  p54, p56-p60, p62, p64, p68-p69, p71, p75-p77, p79, p81, p84-p87.|1589-1549 Ma||||Monzogranites,|
31857|Krackatinny Supersuite|71795|4|Described|p31, p33-p34, p36, p41-p49|Calymmian|Calymmian|Rudall Province. Intrudes the Tabletop Terrane. Petrographic description and geochemsitry are briefly discussed, geodynamic implications are discussed in detail.|ca. 1589-1549 Ma||||Fine- to medium-grained biotite-hornblende toanlites, monzogranites and leucogranites with calcic, calc-alkaline and alkali-calcic I-type compositions.|
31857|Krackatinny Supersuite|73168|5|Briefly described|p743, p745-746, p760, p762-763|early Mesoproterozoic|early Mesoproterozoic|Rudall Province. Tabletop Domain. Shown as Krakatinny Supersuite in Fig. 3, p742. Calc-alkaline, and has geochemical characteristics of A-type magmatism. Only strongly foliated near the Camel-Tabletop Fault Zone. Emplacement associated with metamorphism in the Tabletop Domain recorded by ca 1600-1550 Ma ziron growth. Location in text includes p742 Fig.3.|ca 1590-1550 Ma||||Felsic magmatism, includes tonalite. Deformed and metamorphosed.|
31857|Krackatinny Supersuite|73345|6|Mentioned|p228|||||||||
31776|Krackatinny Tonalite|50436|5|Briefly described|p1.3, 3.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of the Krackatinny Supersuite.||||||
22137|Kudata Dolomite|43563|6|Mentioned|p4|||||||||
22137|Kudata Dolomite|43803|2|Defined|p67|||||||||
22137|Kudata Dolomite|50089|5|Briefly described|p428 Fig. 2, p430 Fig. 5|Ordovician|Ordovician|Geological Province: Canning Basin.||||||04-MAY-05
22137|Kudata Dolomite|64334|5|Briefly described|p39|Ordovician|Ordovician|Eastern Lennard Shelf, Canning Basin. Arenig.||Prices Creek Group.||Overlies Kunian Sandstone. Is overlain by Emanuel Formation.|Dolostone.|
22137|Kudata Dolomite|64580|6|Mentioned|map legend|||Of Prices Creek Group.||||||15-DEC-08
22137|Kudata Dolomite|64643|6|Mentioned|p6|||Of Prices Creek Group.||||||24-NOV-08
22137|Kudata Dolomite|69099|5|Briefly described|500k_geologyp08_lut.csv|Middle Ordovician|Early Ordovician|||Prices Creek Group||||
22137|Kudata Dolomite|69165|6|Mentioned|500k_geologyp08_lut.csv|Ordovician|Ordovician|||Prices Creek Group||||
22137|Kudata Dolomite|69883|5|Briefly described|p4-p5|Arenig|Tremadocian|Canning Basin. Conodont zones and supersequences provided.||Prices Creek Group||Overlies the Kunian Sandstone. Overlain by the Emanuel Formation.|Carbonate and mudstone.|
22137|Kudata Dolomite|71146|6|Mentioned|p24|||Lennard Shelf, Canning Basin.||Prices Creek Group||Equivalent to the Nambeet Formation.||
22137|Kudata Dolomite|71171|6|Mentioned|p2|||Canning Basin.||||||
22137|Kudata Dolomite|73344|5|Briefly described|p3-4, p6, p41, p51, p53, p56, p62-63|Tremadocian|Tremadocian|Canning Basin, Lennard Shelf. Defined by Nicoll et al. (1993). Type section from 88 m, cores 1-3 from BMR Noonkanbah 3 well. Part of supersequence A0. Does not contain datable macrofossils. General age from a conodont species from[?] the Drepanastodus-Paltodus biozone. The P. elegans - B. extensus biozone is also tentatively identified in the Grevillea 1 well on the Lennard Shelf.||Prices Creek Group||Underlain by Kunian Sandstone. Overlain by Emanuel Formation. Equivalent to Fly Flat Member and Samphire Marsh Member (Nambeet Formation) and Wilson Cliffs Sandstone.||
33810|Kulail Sandstone|50286|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin.||||||
33810|Kulail Sandstone|50321|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin.||||||
33810|Kulail Sandstone|60679|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Quartz Sandstone. Geological Province: Amadeus Basin.||||||14-JAN-05
33810|Kulail Sandstone|61154|5|Briefly described|p17|||Basal part of succession that includes Dean Quartzite. Feldspathic and immature sandstone. Grades up into Dean Quartzite in Bloods Range region.  Geological Province: Amadeus Basin.||||||09-OCT-06
33810|Kulail Sandstone|61386|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Red/purple crystalline quartzite sandstone, abundant trough cross beds, locally heavy mineral horizons of hematite and magnetite.  Geological Province: Amadeus Basin.||||||
33810|Kulail Sandstone|62989|5|Briefly described|p39, p40|||Basal unit in Amadeus Basin. Overlain by Dean Quartzite. Comprises deltaic sediments of quartz arenite to quartzofeldspathic beds, with moderately sorted quartz gravel to quartz pebble clasts; grading into finely laminated quartz sandstone layers.||||||25-JAN-07
33810|Kulail Sandstone|65256|2|Defined|piii, p6 Tb.1, p16-17, p40|Cryogenian|Tonian|New name: Disconformably overlies Bloods Range Formation (Tjauwata Group); overlies Amputjuta Dacite, Puntitjata Rhyolite; overlies Pottoyu Granite Suite; conformably underlies (grades into or interfingers with) Dean Quartzite. Formerly mapped as part of the Dean Quartzite. 60-300+m thick. Purple-red to orange, medium-grained crystalline quartz sandstone, sometimes gritty quartzofeldspathic sandstone and minor quartzite, with quartz conglomerate and quartz-muscovite layers, possible rare, poorly preserved mafic volcanics. 850 Ma.||||||
33810|Kulail Sandstone|67565|6|Mentioned|p38.|||In Bloods Range 1:250 000 sheet. A stratigraphic equivalent to the basal interval of the Heavitree Quartzite.||||||
33810|Kulail Sandstone|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|W Amadeus Basin.||||||
33810|Kulail Sandstone|69031|6|Mentioned|p4|||Amadeus Basin.||||||
33810|Kulail Sandstone|69436|6|Mentioned|p21:4|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||12-JUL-16
33810|Kulail Sandstone|69438|5|Briefly described|p23:2-4, 8-9, 18|Cryogenian|Cryogenian|Close et al. (2004). Musgrave Province, Amadeus Basin. Transitional, possibly deltaic deposits. Winnowed heavy mineral horizons sometimes occur.||||Disconformably overlies Bloods Range Formation. Is overlain conformably and gradationally by Dean Quartzite.|Purple-red to orange, medium-grained, generally equigranular quartz to quartzofeldspathic sandstone, containing abundant sedimentary structures. Basal lenses and beds with moderately sorted quartz gravel to quartz pebble clasts.|12-JUL-16
33810|Kulail Sandstone|69606|5|Briefly described|p2, p4 fig 2|Cryogenian|Cryogenian|Southern Amadeus Basin. Potential reservoir rocks.||||Overlain by the Dean Quartzite|Sandstone.|
33810|Kulail Sandstone|69673|6|Mentioned|p63|||||||Overlain by Dean Quartzite||
33810|Kulail Sandstone|70018|5|Briefly described|p234-235,239-240|Neoproterozoic|Neoproterozoic|Amadeus Basin. Of Supersequence 1 in the southern Amadeus Basin. Correlable to Heavitree Quartzite in the northern Amadeus Basin. Deposition occurred during post-rift subsidence after initial uplift of Musgrave Block.||||Overlain by Dean Quartzite. Underlain unconformably by Amadeus Basin stratigraphy.||
33810|Kulail Sandstone|70793|4|Described|500k_interpgeop14_lut.csv + geochron|Cryogenian|Neoproterozoic|Of Amadeus Basin (Phase 1), Centralian Superbasin. Occurs on the SW margin of the Amadeus Basin. Events: Alice Springs Orogeny (450-295 Ma); Areyonga Movement; Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma). Sample GSWA 199407 (sandstone) yielded an interpreted (weighted mean 207Pb*/206Pb*) maximum depositional age of 1119+\-13 Ma. See 500k_interpgeop14_lut.csv, 2_5m_interpgeop15_lut.csv.|1000-800 Ma (inferred; biostrat).|||Overlain by Dean Quartzite. Equivalent to Heavitree Quartzite.|Quartz sandstone, sandstone, and conglomerate; kyanite schist locally|
33810|Kulail Sandstone|70826|6|Mentioned|p5 tbl 2|||Supersequence 1, Centralian Superbasin.||||||20-APR-20
33810|Kulail Sandstone|70839|5|Briefly described|p328-334,336|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Basal unit of Supersequence 1; Equivalent to Dean Quartzite, and Heavitree Quartzite to the north. Exposed as part of 30-60km wide belt of ranges immediate south of southern limit of Supersequence 4 deposits. SHRIMP U-Pb zircon geochronology samples and analysis on p331-334. Detrital zircon age spectrum range between c. 1.82 and 1.09 Ga (Warakurna Supersuite), with dominant age component at 1.22-1.1 Ga (derived from Pitjantjatjara Supersuite; Musgrave orogeny). Older age peak at c. 1.73 Ga.|Max dep age: 1092+\-11 Ma (207Pb/206Pb)|||Overlain by Dean Quartzite. Correlable to Heavitree and Dean Quartzites.||
33810|Kulail Sandstone|71080|6|Mentioned|p23, 30|Tonian|Tonian|Southern Amadeus Basin. WA only? Base of Supersequence 1.||||Correlated with Munyu Sandstone, Murraba Basin.|Dominantly sandstone.|
33810|Kulail Sandstone|71088|6|Mentioned|p4, p6-p8, p10, p17|Mesoproterozoic|Mesoproterozoic|Amadeus Basin. Part of Supersequence 1.|c. 1200-1150 Ma|||||
33810|Kulail Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
33810|Kulail Sandstone|71268|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Of Amadeus Basin (Phase 1), Centralian Superbasin. Events: Delamerian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma). Sample GSWA 199407 (quartz-rich sandstone) yielded a weighted mean 207Pb/206Pb age of 1119+\-13 Ma, interpreted as maximum depositional age of the sandstone. See 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeol_lut.csv.|976-827 Ma (inferred)|||Overlain by Dean Quartzite. Correlable with Heavitree Quartzite, Vaughan Springs Quartzite.|Fine- to coarse-grained, purple-red  quartz- and quartzofeldspathic metasandstone containing heavy mineral bands; locally interbedded with quartzite and poorly sorted, polymictic pebble metaconglomerate; abundant sedimentary structures.|
33810|Kulail Sandstone|71279|6|Mentioned|p355 Fig.2|Cryogenian|Cryogenian|Amadeus Basin.||||||
33810|Kulail Sandstone|71592|5|Briefly described|Appendix A.|||Amadeus Basin.|1119+/-13 Ma (MDA: U-Pb zircon SHRIMP)||||Fine-grained quartz sandstone.|
33810|Kulail Sandstone|71841|5|Briefly described|p1|Cryogenian|Cryogenian|Of Amadeus Basin.||||Overlain by, and grades into Dean Quartzite. Underlain by basement.||
33810|Kulail Sandstone|71842|6|Mentioned|p3|Cryogenian|Cryogenian|Of Amadeus Basin.||||||
33810|Kulail Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Tonian|Tonian|Amadeus Basin (Phase 1). Informal grouping of mostly time-equivalent silicilastic units. Grouped with Dean Quartzite, Heavitree Quartzite, and Vaughan Springs Quartzite. Min age  from biostratigraphy.|||||Informal grouping description: Quartz sandstone, sandstone, and conglomerate; kyanite schist locally [probably only in Dean Quartzite].|
33810|Kulail Sandstone|72094|6|Mentioned|p3 Fig 2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
33810|Kulail Sandstone|72601|6|Mentioned|p3|Tonian|Tonian|Amadeus Basin. Found in the southern part of the basin.||||||
33810|Kulail Sandstone|73085|6|Mentioned|p1|Tonian|Stenian[?]|||||Overlain by Dean Quartzite.||
33810|Kulail Sandstone|73086|6|Mentioned|p7, p9, p145|||Amadeus Basin. Part of Supersequence I[?]; deposited during the early sag phase of basin development. Restricted to exposures in the southwest of the basin.||||Correlates to Heavitree Formation[?].||
33810|Kulail Sandstone|73346|6|Mentioned|p5|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
33810|Kulail Sandstone|73437|6|Mentioned|p151|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
25725|Kulele Limestone|23529|5|Briefly described|p10|||Parent: Miningarra Subgroup.   Geological Province: Earaheedy Basin||||||
25725|Kulele Limestone|23589|6|Mentioned|p2 fig 1|||Possibly variation of Kulele Creek Limestone. Of Miningarra Subgroup. Earaheedy Basin.||||||
25725|Kulele Limestone|23890|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Of Miningarra Subgroup. Geological Province: Earaheedy Basin.||||||07-NOV-08
25725|Kulele Limestone|24017|5|Briefly described|p3 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Miningarra Subgroup.  Geological Province: Earaheedy Basin.||||||07-NOV-08
25725|Kulele Limestone|24578|4|Described|p776 Fig.1, p781|Paleoproterozoic|Paleoproterozoic|Of the Miningarra Subgroup (Earaheedy Group). Overlain by the Mulgarra Sandstone. Overlies the Wongawol Formation. Geological Province: Earaheedy Basin||||||07-NOV-08
25725|Kulele Limestone|30010|6|Mentioned|p45|||Variation of Kulele Creek?||||||
25725|Kulele Limestone|37021|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25725|Kulele Limestone|38515|6|Mentioned|p9|||||||||
25725|Kulele Limestone|38988|6|Mentioned|Fig.2|||||||||
25725|Kulele Limestone|39894|5|Briefly described|Fig.2|||||||||
25725|Kulele Limestone|40354|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25725|Kulele Limestone|40355|5|Briefly described|p7|||||||||
25725|Kulele Limestone|40934|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25725|Kulele Limestone|40938|1|Redefined|p60|Paleoproterozoic|Paleoproterozoic|Redefinition of Kulele Creek Limestone.||||||07-NOV-08
25725|Kulele Limestone|40939|5|Briefly described|p108|||||||||
25725|Kulele Limestone|42548|5|Briefly described|p52|||||||||
25725|Kulele Limestone|50188|5|Briefly described|p2  Fig. 1, p3|||Of the Miningarra Subgroup (Earaheedy Group).  Geological Province: Earaheedy Basin.  Maximum Thickness: ~300m.||||||16-JUL-08
25725|Kulele Limestone|50222|4|Described|p320 Fig. 3, p329|Paleoproterozoic|Paleoproterozoic|Of the Earaheedy Group. Consists of carbonate units (stromatolitic, oolitic and pisolitic), separated by shale and sandstone. Max. thickness: ~300m.  Geological Province: earaheedy Basin.||||||07-NOV-08
25725|Kulele Limestone|50223|5|Briefly described|p345 Fig. 2, p348|Paleoproterozoic|Paleoproterozoic|Of the Miningarra Subgroup (Earhaeedy Group).  Interbedded carbonate, shale and sandstone units.  Max. thickness: 300m.  Geological Province: Earaheedy Basin.||||||07-NOV-08
25725|Kulele Limestone|50224|5|Briefly described|p368 Tb.1|Paleoproterozoic|Paleoproterozoic|Of the Minningarra Subgroup (Earaheedy Group). Oolitic, pisolitic, stromatolitic and brecciated limestone; calcarenite, sandstone, siltstone. Max. thickness: ~300m. Geological Province: Earaheedy Basin.||||||07-FEB-11
25725|Kulele Limestone|50226|5|Briefly described|p423, p424 Fig. 5|||Of the Miningarra Subgroup (Earaheedy Group).  Geological Province: Earaheedy Basin.||||||09-DEC-04
25725|Kulele Limestone|63866|5|Briefly described|p166|||Eraheedy Basin.||Miningarra Subgroup||Overlies the Wongawol Formation. Overlain by the Mulgarra Sandstone.||
25725|Kulele Limestone|64284|4|Described|p58 Fig. 1, p60 Fig. 2, p61|Paleoproterozoic|Paleoproterozoic|Of the Minningarra Subgroup (Earaheedy Group). Thickness: up to 300m. Geological Province: Earaheedy Basin. Cyclic platform succession of carbonate units separated by shale and sandstone.||||||07-FEB-11
25725|Kulele Limestone|64580|4|Described|map legend||Paleoproterozoic|Of Miningarra Subgroup. Stromatolitic limestone, micaceous siltstone, mudstone, and fine-grained sandstone.||||||09-DEC-08
25725|Kulele Limestone|64725|6|Mentioned|p59.|||||Unit in Miningarra Subgroup.||Overlies Wongawol Formation. Is overlain by Mulgarra Sandstone.||03-APR-12
25725|Kulele Limestone|64772|4|Described|p12, Plate 1  legend, p10 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of Earaheedy Gp.Overlies Wongawol Fm gradationally. Thickness: ~300m. Geol.prov: Earaheedy Basin. Various interbedded limestone types forming crude cyclic sequences separated by thicker units of micaceous shale, mudst. + fine-gr.sst - more lith.details. On Plate 1,  unit is of Earaheedy Group (as Miningarra Subgroup not shown). See also p19 Fig.9, p20-21 Fig.10, p26 Fig.13, p69 App.4, p75 App.4 Tb.4.3, p76-77 Fig.4.2, p78 App.4 Tb.4.4, p79-81 App.4 Fig.4.3,||||top of unit is marked by base of thick quartz arenite of Mulgarra Sandstone.||25-NOV-13
25725|Kulele Limestone|65472|5|Briefly described|p1, p3 Fig.2, p5 Fig. 4|||Thickness: ~300 m. Earaheedy Basin. On p3 Fig.2, Miningarra Subgroup range not shown to include Kulele Limestone and Mulgarra Sandstone.||Miningarra Subgroup||||
25725|Kulele Limestone|65692|5|Briefly described|p9-10, p55|||Sub-tidal to inter-tidal environment of deposition. Is listed as [Kulele] Formation on p9.||Miningarra Subgroup.||Overlies Wongawol Formation. Is overlain by Mulgarra Sandstone.|Includes cyclic layers of carbonate, shale and siltstone (attributed to changes in sea level).|
25725|Kulele Limestone|66427|6|Mentioned|p43 Fig.2, p46-47, p51, p68-73      |||c.300 m thick.||Unit in Miningarra Subgroup.||Overlies Wongawol Formation. Is overlain by Mulgarra Sandstone.|A cyclic platform succession of interbedded calcarenite, stromatolitic limestone, intraclastic carbonate breccia, oolitic and pisolitic limestone, siltstone and sandstone.|
25725|Kulele Limestone|67855|6|Mentioned|p208 fig 3-8, p209|Paleoproterozoic|Paleoproterozoic|||Minningarra Subgroup|||Carbonate with giant stromatolites.|
25725|Kulele Limestone|68055|6|Mentioned|p77|Proterozoic|Proterozoic|Earaheedy Basin.||Miningarra Subgroup.||||
25725|Kulele Limestone|69003|5|Briefly described|p13 Fig.17, p14|||Earaheedy Basin. c.300m thick.||Miningarra Group.||Conformably? overlies Wongawol Formation. Is overlain conformably? by Mulgarra Sandstone.|Stromatolitic limestone.|
25725|Kulele Limestone|69313|6|Mentioned|p22 Fig.4.2, p25|Paleoproterozoic|Paleoproterozoic|||Minningarra Subgroup||Overlies the Wongawol Formation. Overlain by the Mulgarra Sandstone.|Limestones.|08-SEP-17
25725|Kulele Limestone|69596|6|Mentioned|p10-11|||Earaheedy Basin.||Miningarra Group.||||
25725|Kulele Limestone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||calcarenite, mudstone, shale, limestone|
25725|Kulele Limestone|71484|4|Described|p124-125,131-132,137-138|Orosirian|Orosirian|Geological province: Of Earaheedy Basin. Thickness: ~600m thick, based on measured section. A cyclic shallow-water platform succession. Deposited prior to c. 1820 Ma Capricorn Orogeny along northern Yilgarn margin.||Unit of Miningarra Group.||Overlain by Mulgarra Sandstone. Underlain by Wongawol Formation.|Stromatolitic limestone, intraclastic carbonate breccia, calcarenite, limestone, siltstone, sandstone.|30-AUG-19
25725|Kulele Limestone|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin.|Max age 1876+/-19 Ma, Min ~1650 Ma.|Miningarra Group|||Stromatolitic limestone, micaceous siltstone, mudstone, and fine-grained sandstone; common metre-scale cyclicity.|
73260|Kulkatharra Dolerite|64580|4|Described|map legend||Mesoproterozoic|Of Warakurna Supersuite. Dolerite and gabbro sills intruded into Edmund Group and Collier Group.||||||15-DEC-08
73260|Kulkatharra Dolerite|66104|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Dolerite and gabbro sills which intrude into the Edmund and Collier Groups. Age shown as c.1070 Ma.||||||
73260|Kulkatharra Dolerite|66112|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Aged c.1070 Ma. Dolerite and gabbro sills intruded into Edmund Group and Collier Group.||||||
73260|Kulkatharra Dolerite|66241|5|Briefly described|pp1-4, p9. |Stenian|Stenian||1070 Ma.|||Intrudes Edmund Group and Collier Group.||
73260|Kulkatharra Dolerite|66299|6|Mentioned|p6 Fig.3, p333.|||||||Intrudes into Edmund and Collier Groups. Cut across by dykes of Mundine Well Dolerite Suite.||
73260|Kulkatharra Dolerite|66887|5|Briefly described|p5 Fig.4|Mesoproterozoic|Mesoproterozoic|Southern Gascoyne Province.|~1070 Ma estimated from Fig.4.|||||
73260|Kulkatharra Dolerite|66950|6|Mentioned|p9 Fig.8|Stenian|Stenian||c. 1100-1000 Ma|||||
73260|Kulkatharra Dolerite|67136|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|c.1070 Ma.|Unit in Warakurna Supersuite.||Intrudes Edmund and Collier Groups.|Dolerite and gabbro sills intruded into Edmund Group and Collier Group.|
73260|Kulkatharra Dolerite|67374|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|c.1070 Ma.|||Intrudes Edmund and Collier Groups.|Dolerite and gabbro sills.|
73260|Kulkatharra Dolerite|68285|5|Briefly described|Map Legend|Stenian|Stenian|Of Warakurna Large Igneous Province|c. 1070 Ma|||Intrudes into Edmund Group and Collier Group.|Dolerite and gabbro sills.|
73260|Kulkatharra Dolerite|68286|5|Briefly described|Map Legend|Stenian|Stenian|Of Warakurna Large Igneous Province|c. 1070 Ma|||Intrudes into Edmund Group and Collier Group.|Dolerite and gabbro sills.|
73260|Kulkatharra Dolerite|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Mesoproterozoic|||Warakurna Supersuite||Intruded into Edmund Group and Collier Group|Dolerite and gabbro sills|
73260|Kulkatharra Dolerite|69003|5|Briefly described|p4, p34, p48, p53|||Bangemall Basin, Capricorn Orogen. Part of the Warakurna LIP.|c.1070 Ma.|||Intrudes Ilgarari Formation (Collier Group).||
73260|Kulkatharra Dolerite|69010|5|Briefly described|Map Legend|Stenian|Stenian||c. 1070 Ma|Of the Warakurna Supersuite.||Intrudes the Edmund and Collier Groups.|Dolerite and gabbro sills.|24-APR-14
73260|Kulkatharra Dolerite|69028|5|Briefly described|Map Legend|Stenian|Stenian||c. 1070 Ma|||Intrudes the Edmund Group and the Collier Group.|Dolerite and gabbro sills.|06-MAY-14
73260|Kulkatharra Dolerite|69080|5|Briefly described|p684, p690-691, p698|Stenian|Stenian|Gascoyne Province. Part of the Warakurna Large Igneous Province.|c.1070 Ma.|||Intrudes Edmund and Collier Groups.|Dolerite and gabbro sills intruded into Edmund and Collier Groups.|
73260|Kulkatharra Dolerite|69091|5|Briefly described|p202|||widely intrudes the Collier Basin|ca. 1070 Ma|||||
73260|Kulkatharra Dolerite|69166|4|Described|geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|||Warakurna Supersuite|||Dolerite and gabbro sills intruded into Edmund Group and Collier Group|
73260|Kulkatharra Dolerite|69185|4|Described|500k_geologyp08_lut.csv||Mesoproterozoic|Geological Province: Pilbara Craton.||Unit of Warakurna Supersuite.||Intrudes into Edmund and Collier Groups.|Dolerite and gabbro sills,|
73260|Kulkatharra Dolerite|69596|5|Briefly described|p4-5, p12 Fig.7, p13|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.|c.1070 Ma.|Warakurna Supersuite.||Intrudes Edmund and Collier Groups.||
73260|Kulkatharra Dolerite|70019|6|Mentioned|p94|||Geological province: Gascoyne Province, Capricorn Orogen. |c. 1070 Ma|||||
73260|Kulkatharra Dolerite|70132|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Collier Basin. Warakurna Large Igneous Province.||||Intrudes Edmund and Collier Groups.|Dolerite and gabbro sills intruded into Edmund and Collier Groups.|10-NOV-15
73260|Kulkatharra Dolerite|70136|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|c.1070 Ma.|Warakurna Supersuite.||Intrudes Edmund and Collier Groups.|Dolerite and gabbro sills intruded into Edmund and Collier Groups.|
73260|Kulkatharra Dolerite|70767|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|1084-1067 Ma.|Warakurna Supersuite.||Intrudes Edmund and Collier Groups.|Dolerite and gabbro sills intruded into Edmund and Collier Groups.|
73260|Kulkatharra Dolerite|70768|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|1084-1067 Ma.|Warakurna Supersuite.||Intrudes Edmund and Collier Groups.|Dolerite and gabbro sills intruded into Edmund and Collier Groups.|
73260|Kulkatharra Dolerite|70795|5|Briefly described|100k_geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Also 100k_geologyl_lut.csv, 500k_interpgeol_lut.csv, 189218.1.pdf|1084-1067 Ma|Warakurna Supersuite||Intrudes Edmund Group and Collier Group, Ullawarra Formation|Dolerite and gabbro sills.|
73260|Kulkatharra Dolerite|70796|5|Briefly described|500k_interpgeop14_lut.csv|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|ca 1070 Ma (inferred)|Warakurna Supersuite||Intruded into Edmund Group and Collier Group|Dolerite and gabbro sills.|
73260|Kulkatharra Dolerite|70814|5|Briefly described|p3, p5, p14-p15, p22, p26, p37, p39, p41|Calymmian|Calymmian|Edmund Basin. A Baddeleyite age of 1068 +/- 22 Ma is derived by Wingate (2002).|1084-1067 Ma|||Intrudes the Blue Billy and Ullawarra Formations. Intrudes the Edmund and Collier Groups.||
73260|Kulkatharra Dolerite|70826|6|Mentioned|p10|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||Warakurna Supersuite.||||20-MAY-20
73260|Kulkatharra Dolerite|71158|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|1084-1067 Ma.|||Intrudes Collier and Edmund Groups.|Dolerite and gabbro sills.|
73260|Kulkatharra Dolerite|71210|6|Mentioned|p5, p11|||||Warakurna Supersuite||||
73260|Kulkatharra Dolerite|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||dolerite, gabbro|
73260|Kulkatharra Dolerite|71269|4|Described|500k_interpgeop16_lut.csv|Mesoproterozoic|Mesoproterozoic|Of Collier Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Edmundian Orogeny (1026-954 Ma); Warakurna Supersuite Magmatic Event (1084-1040 Ma); Giles Event (1085-1040 Ma).|1984+\-6 Ma; 1067+\-134 Ma (isotopic)|||Intruded into Edmund Group and Collier Group.|Dolerite and gabbro sills|
73260|Kulkatharra Dolerite|71484|6|Mentioned|p125|||Geological province: Of Edmund and Collier basins. Intruded into Edmund and Collier groups.|||||Dolerite and gabbro sills.|30-AUG-19
73260|Kulkatharra Dolerite|71869|6|Mentioned|p4||||c. 1100 Ma|||||
73260|Kulkatharra Dolerite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Collier Basin, Capricorn Orogen.|Max age 1084+/-6 Ma, min 1067+/-14 Ma|Warakurna Supersuite|||Dolerite and gabbro sills intruded into Edmund Group and Collier Group.|
73260|Kulkatharra Dolerite|72259|6|Mentioned|p3|Stenian|Stenian||ca. 1070 Ma|||||
73260|Kulkatharra Dolerite|72705|6|Mentioned|p14||||c.1070 Ma.|||||
73260|Kulkatharra Dolerite|73102|4|Described|p1-7, p10-11, p14-26, p28-31|Stenian|Stenian|Gascoyne Province; Capricorn Orogen. A component of the c. 1075 Ma Warakurna Large Igneous Province. Form extensive dolerite sills within sedimentary rocks of the Edmund and Collier Groups. Unit previously defined on the basis of dolerite sills alone. U-Pb geochronology confirms that the dykes and sills are contemporaneous; dykes may be feeders for the sills based on similar mineralogy and geochemistry. Dykes also intrude the southern Ashburton and Blair basins. The majority of dykes appear to terminate against the Talga - Mount Vernon Fault System and the Godfrey Fault. Similar trend to Mundine Well Dolerite dykes in the western parts of the Ullawarra and Edmund map sheets, which makes them difficult to distinguish based on orientation alone. Dykes are mostly nothwest or northeast trending and some are east-west; interpreted strike lengths of 3-70 km and are mainly 1-20 m wide (rarely up to 150 m). Dykes comprise two distinct petrographic types. Dykes are significantly less altered and metamorphosed than those of Narimbunna Dolerite and Minga [Dolerite]. Sills fall into one of three groups defined by distinct trends in Th/Yb vs Nb/Yb. [Article includes detailed petrographic description, whole rock major and trace element composition, Sm-Nd isotope composition].|1083-1075 Ma|||Intrudes Edmund Group, Collier Group, Bresnahan Group, Capricorn Group, Wyloo Group, Durlacher Supersuite, Pooranoo Metamorphics, Leake Spring Metamorphics. Intruded by Mundine Well Dolerite.|Dykes: mainly quartz dolerite, moderately altered to unaltered, locally porphyritic. Sills: typically quartz dolerite, locally porphyritic, relatively unaltered, and medium to coarse. Localised coarse-grained to pegmatitic granophyric segregations.|
73260|Kulkatharra Dolerite|73442|4|Described|p1-3, p5-6, p9-13, p16-17, p19-27|Stenian|Stenian|Capricorn Orogen, Edmund and Collier Basins. Component of the Warakurna Large Igneous Province. Weighted mean age of 1075+/-3 Ma from three samples. Older ages of 1081+/-6 and 1084+/-5 Ma may represent a separate intrusive event. Intrudes Edmund Group Depositional Packages 1-4 in NW part of Capricorn Orogen, elsewhere intrudes the Collier Group Depositional Packages 5 and 6. Comprises voluminous, laterally continuous (up to 210km long) sills, may be up to 600m thick in the eastern Capricorn Orogen. Mostly conformable with host rocks, the sills are also regionally discordant along strike. Rare dolerite margin textures indicate some sills were emplaced at shallow depths. Characterised mostly as a sub-alkaline, high-Fe tholeiitic basalt, enriched in REE and HFSE. Appears as Kulkatharra Dolerites p23. Location in text includes iii-iv, p14 Fig.12, p15 Fig.13-14, p35-39.|1083-1067 Ma U-Pb zircon and baddeleyite|||Intruded into Edmund Group, Collier Group|Dolerite and gabbro sills. Typically fine- to coarse-grained, equigranular to subophitic quartz dolerite, central to upper parts of the sills commonly contain coarse-grained to pegmatitic granophyric segregations. Slightly weathered.|
79625|Kullal Dolerite|68996|6|Mentioned|p6|||||||||
79625|Kullal Dolerite|69640|6|Mentioned|p11|Proterozoic|Proterozoic|Musgrave Province.||||Intrudes the Pitjantjatjara Supersuite.||
79625|Kullal Dolerite|71321|6|Mentioned|p1,22-23|||Geological province: Musgrave Province. See Kullal Dyke Suite.||||||24-OCT-19
79625|Kullal Dolerite|73184|6|Mentioned|p196|Tonian?|Stenian|Potential source of Neoproterozoic detrital zircons in the Grant Group.|ca 1000 Ma|||||
23707|Kumina Conglomerate|38776|2|Defined|p40|middle Pleistocene|early Pleistocene|Early-Mid Pleistocene.||||||07-APR-16
23707|Kumina Conglomerate|40987|4|Described|p34|||||||||
23707|Kumina Conglomerate|61155|5|Briefly described|p16|Late Pliocene|Middle Miocene|Overlies the Wiluna Hardpan. Age: ~14-~2Ma.  Thickness: 100m. Geological Province: West Fortescue Valley.||||||
23707|Kumina Conglomerate|63372|5|Briefly described|Map Legend|Middle Pleistocene|Early Pleistocene|Alluvial fan deposits, partly cemented.||||||
23707|Kumina Conglomerate|65194|5|Briefly described|p15-16 Figs.2.3, 2.4, p.101-106, p.108|Pleistocene|Neogene|A Neogene alluvial fan deposit: forms the piedmont slope of the Hamersley Range. 90 m of loosely cemented boulders, cobbles, gravel and sand in a brown silty-clay matrix; ferruginous at base. Fortescue Palaeovalley aquifer. May interfinger in part with Kangiangi Clay.||||Unconformably overlies the Millstream Dolomite, Wittenoom Dolomite, Weelumurra Beds.||07-APR-16
32218|Kunagunarrina Formation|23416|5|Briefly described|Map Legend|Archean|Archean|Of Sulphur Springs Group. Geological Province: Pilbara Craton.||||||15-APR-13
32218|Kunagunarrina Formation|23755|4|Described|p37|Archean|Archean|See also page 17 table 1.  Of Sulphur Springs Group.||||||07-NOV-08
32218|Kunagunarrina Formation|23783|5|Briefly described|p16|Archean|Archean|Of Sulphur Springs Group.||||||07-NOV-08
32218|Kunagunarrina Formation|23891|5|Briefly described|p90|Archean|Archean|Of Sulphur Springs Group. Geological Province: Pilbara Craton. See also page 95.||||||07-NOV-08
32218|Kunagunarrina Formation|23956|5|Briefly described|p1264|||Of the Sulphur Springs Group. Geological Province: Pilbara Craton.||||||
32218|Kunagunarrina Formation|24025|4|Described|p8 Tb. 1|Archean|Archean|Of Sulphur Springs Group.  Pillow basalt, komatiite, high-Mg basalt, and chert.  Max. thickness: 3000 m.  Geological Province: Pilbara Craton.||||||07-NOV-08
32218|Kunagunarrina Formation|24184|5|Briefly described|p702, p699 Fig.4|Archean|Archean|Of the Sulphur Springs Group. Overlain by Kangaroo Caves Formation. Underlain by Leilira Formation. Geological Province: Pilbara Craton. Max Thickness: 2.4km||||||07-NOV-08
32218|Kunagunarrina Formation|24186|5|Briefly described|p777|Archean|Archean|Parent: Sulphur Springs Group. Geological Province: Pilbara Craton.||||||07-NOV-08
32218|Kunagunarrina Formation|24187|5|Briefly described|p777|Archean|Archean|Of the Sulphur Springs Group.||||||07-NOV-08
32218|Kunagunarrina Formation|24531|4|Described|p19|Archean|Archean|Of the Sulphur Springs Group. Composed dominantly of komatiitic, high-Mg and tholeiitic metabasalt, metamorphosed to greenschist facies.  Max. thickness: 1750m.  Conformably overlain by Kangaroo Caves Formation. Geological Province: Pilbara Craton.||||||07-NOV-08
32218|Kunagunarrina Formation|24532|5|Briefly described|Map legend|Archean|Archean|Of the Sulphur Springs Group (Pilbara Supergroup).  Age: c.3240Ma.||||||07-NOV-08
32218|Kunagunarrina Formation|24550|5|Briefly described|p31 Tb. 3.1|Archean|Archean|Of the Sulphur Springs Group. Pillow basalt, high-Mg basalt, chert. Max. thickness: 2.4km. Geological Province: Pilbara Craton.||||||07-FEB-11
32218|Kunagunarrina Formation|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Of the Sulphur Springs Group.||||||07-FEB-11
32218|Kunagunarrina Formation|50379|5|Briefly described|Map Legend|Archean|Archean|Of Sulphur Springs Group (Pilbara Supergroup). Geological Province: Pilbara Craton.||||||07-NOV-08
32218|Kunagunarrina Formation|61256|5|Briefly described|p340 Fig. 5a|Archean|Archean|Of the Sulphur Springs Group.  Ultramafic volcanic rocks.  Overlies the Leilira Formation.||||||07-NOV-08
32218|Kunagunarrina Formation|61266|4|Described|p58 Tb.1, p59|Archean|Archean|Of Sulphur Springs Group. Overlies Leilira Formation. Overlain by Kangaroo Caves Formation. Pillow basalt, komatiite, high Mg-basalt, chert. Max. thickness: ~3000m. Geological Province: Pilbara Craton.||||||07-NOV-08
32218|Kunagunarrina Formation|61579|5|Briefly described|p58 Fig. 2|Archean|Archean|Of the Sulphur Springs Group. ||||||07-NOV-08
32218|Kunagunarrina Formation|63420|5|Briefly described|Map legend|Archean|Archean|Of Sulphur Springs Group ( Pilbara Supergroup). Geological Province: Pilbara Craton. Shale, wacke and sandstone; altered komatiitic basalt locally at base; metamorphosed.||||||07-NOV-08
32218|Kunagunarrina Formation|63538|4|Described|p10, p6 Fig. 3|Archean|Archean|Of Sulphur Springs Group. Underlain by Leilira Formation, overlain by Kangaroo Caves Formation. Geol Prov: Pilbara Craton. Weakly metamorphosed mafic-ultramafic lavas, a lower and middle units of weathering basalt to komatiitic basalt.||||||19-APR-13
32218|Kunagunarrina Formation|64328|5|Briefly described|p56 Tb. 1|||Of Sulphur Springs Group.  Ultramafic rock, basalt.||||||07-FEB-11
32218|Kunagunarrina Formation|64405|5|Briefly described|p4 Fig. 3|Archean|Archean|Name inferred from Kunungunarrina only in Figure 3. Of the Sulphur Springs Group (De Grey Supergroup). Age: between 3251-3235Ma and </-3273-3255Ma.||||||07-FEB-11
32218|Kunagunarrina Formation|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Sulphur Springs Group. Basaltic volcanic rocks, with minor komatiite, siliciclastic sedimentary rocks, and chert; metamorphosed.||||||
32218|Kunagunarrina Formation|67130|5|Briefly described|p16|Paleoarchean|Paleoarchean|Up to 2000m thick|c. 3250 Ma|Sulphur Springs Group||Overlies Leilira Formation, overlain by Kangaroo Caves Formation|Komatiite and komatiitic basalt.|
32218|Kunagunarrina Formation|67197|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Sulphur Springs Group.||||
32218|Kunagunarrina Formation|67668|6|Mentioned|Fig. 2;||Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Sulphur Springs Group||Overlies the Leilira Formation, underlies the Kangaroo Caves Formation.||
32218|Kunagunarrina Formation|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. The 6 facies are mapped separately.||Of the Sulphur Springs Group.|||Shale; cobble to pebble conglomerate; quartz-rich sandstone; wacke; white-, blue-black-, and grey-layered chert; pillowed flows of komatiitic basalt; all metamorphosed.|23-SEP-13
32218|Kunagunarrina Formation|68282|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. 8 facies are mapped separately.||Of the Sulphur Springs Group|||Mafic schists; white, blue-black and grey layered chert; komatiitic basalt, massive and pillowed flows or local pyroxene spinifex texture; coarse-grained mafic volcaniclastic rocks.|03-DEC-14
32218|Kunagunarrina Formation|68283|5|Briefly described|Map Legend|Archean|Archean|East Pilbara Terrane, Pilbara Craton.||Of the Sulphur Springs Group.|||Shale, wacke, and sandstone; altered komatiitic basalt locally at base; metamorphosed.|23-SEP-13
32218|Kunagunarrina Formation|69013|6|Mentioned|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane. Includes 9 facies mapped separately. See map legend for a detailed lithological description.||Of the Sulphur Springs Group.|||Mafic volcanic rock, chert, basalt, komatiite; all metamorphosed.|30-APR-14
32218|Kunagunarrina Formation|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Mapped as 14 separate unnamed sub-units. See map legend for a detailed lithological description.||Of the Sulphur Springs Group.|||Carbonate-altered metamafic volcanic rocks; ultramafic and mafic schist; interlayered mafic volcanic rock and schist; layered chert; shale; dacite; basalt; komatiite and basaltic komatiite.|02-MAY-14
32218|Kunagunarrina Formation|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Interlayered mafic volcanics and mafic schists. Komatiite with pyroxene spinifex texture and basaltic komatiite. Dacite, metabasalt and meta komatiitic basalt.||Sulphur Springs Group|||Metamafic volcanic rock, mafic schist interlayered with ultramafic schist. Shale, local wacke, sandstone, siltstone/banded iron formation; metamorphosed. Cobble-pebble conglomerate. Quartz sandstone, wacke with volcaniclastic sandstone and shale.|
32218|Kunagunarrina Formation|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.|3255-3245 Ma (inferred)|Unit of Sulphur Springs Group.|||Basalt, chert, komatiitic basalt, conglomerate, interlayered mafic and ultramafic volcanic rocks and schists, komatiite and basaltic komatiite, quartz-rich sandstone, siltstone, shale, banded iron-formation, conglomerate.|
32218|Kunagunarrina Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Sulphur Springs Large Igneous Province, East Pilbara Terrane.|Max age ~3275 Ma, min age 3255+/-3 Ma.|Sulphur Springs Group|||Basaltic rocks with komatiitic basalt; minor komatiite, siliciclastic rocks and chert; metamorphosed.|
32218|Kunagunarrina Formation|72668|5|Briefly described|p5, p6|||East Pilbara Terrane. See also Kunagunarinna Formation p4. Up to 2000m thick.|c. 3250 Ma|Sulphur Springs Group||Overlies the Leilira Formation. Overlain by the Kangaroo Caves Formation.|Komatiite and komatiitic basalt.|
26674|Kunderong Sandstone|34135|5|Briefly described|Table 2|||Bresnahan Group.||||||
26674|Kunderong Sandstone|36883|4|Described|p144|||||||||
26674|Kunderong Sandstone|36902|6|Mentioned|p15|||||||||
26674|Kunderong Sandstone|37460|5|Briefly described|p156|||||||||
26674|Kunderong Sandstone|38298|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Lower Proterozoic||||||07-NOV-08
26674|Kunderong Sandstone|38299|6|Mentioned|p7|||||||||
26674|Kunderong Sandstone|38482|6|Mentioned|p15|||||||||
26674|Kunderong Sandstone|40554|5|Briefly described|p30|||||||||
26674|Kunderong Sandstone|41125|6|Mentioned|p28|||||||||
26674|Kunderong Sandstone|42260|6|Mentioned|p100|||||||||
26674|Kunderong Sandstone|42471|6|Mentioned|p18|||Used 1965||||||
26674|Kunderong Sandstone|44141|6|Mentioned|p304-308|||The Cherrybooka Conglomerate and Kunderong Sandstone intergrade laterally and vertically; therefore they are not clearly mappable.||Bresnahan Group||Overlies gradationally Cherrybooka Conglomerate.||
26674|Kunderong Sandstone|69028|5|Briefly described|Map Legend|Calymmian|Statherian|Bresnahan Basin. Mapped with Cherrybooka Conglomerate as a single unit.||Of the Bresnahan Group.|||Pebble- to boulder-conglomerate, pebbly sandstone, sandstone, siltstone and mudstone.|07-MAY-14
26271|Kungarra Formation|23045|6|Mentioned|291|||Parent Turee Creek Group||||||
26271|Kungarra Formation|23047|5|Briefly described|38|||Of the Turee Creek Group. Hamersley Province.  Max thickness 2.8 km. Overlain by Koolbye Formation.||||||10-FEB-09
26271|Kungarra Formation|23280|5|Briefly described|p1089,Table1p1085||Siderian|Max Age: 2449 (+/-) 3 Ma.||||||
26271|Kungarra Formation|23570|5|Briefly described|p14|Archean|Archean|Of Turee Creek Group. Geological Province: Pilbara Craton||||||23-MAR-09
26271|Kungarra Formation|23612|5|Briefly described|p840|Archean|Archean|Of Turee Creek Group.||||||23-JUN-09
26271|Kungarra Formation|23890|4|Described|p16|Paleoproterozoic|Archean|Of Turee Creek Group. Geological Province: Pilbara Craton.  Maximum thickness: ~2000m.||||||07-NOV-08
26271|Kungarra Formation|24544|4|Described|p47 Fig.35|Paleoproterozoic|Paleoproterozoic|Of the Turee Creek Group. Conformably overlies Boolgeeda Formation. Conformably overlain by Koolbye Formation. Geological Province: Hamersley Basin.||||||07-NOV-08
26271|Kungarra Formation|24607|5|Briefly described|p969 Fig. 2|||Of the Turee Creek Group.||||||
26271|Kungarra Formation|35976|2|Defined|p110|Proterozoic|Proterozoic|||||||
26271|Kungarra Formation|36902|6|Mentioned|p15|||||||||
26271|Kungarra Formation|37327|3|Fully described|p395|||||||||
26271|Kungarra Formation|37934|6|Mentioned|p555|||Contains Meteorite Bore Member.||||||23-JUN-09
26271|Kungarra Formation|38482|6|Mentioned|p15|||||||||
26271|Kungarra Formation|42190|5|Briefly described|p274|||||||||
26271|Kungarra Formation|42898|5|Briefly described|Fig.2 P341|||||||||
26271|Kungarra Formation|43037|5|Briefly described|p26|||of Turee Creek Group||||||
26271|Kungarra Formation|43262|5|Briefly described|Map Legend||Proterozoic|of Turee Creek Group.||||||
26271|Kungarra Formation|43290|4|Described|p7||Proterozoic|Of Turee Creek Group.||||||23-MAR-09
26271|Kungarra Formation|44152|5|Briefly described|p188 Fig.2-161, p189|||||Turee Creek Group (base of).|Meteorite Bore Member.|Overlies Boolgeeda Iron Formation (conformably).|Monotonous sequence of greyish-green siltstone; fine-grained greywacke; and fine-grained sandstone; thin carbonate beds in upper part, and abundant dolerite sills.|
26271|Kungarra Formation|60373|5|Briefly described|p145 Tb. 1|||Of Turee Creek Group. Overlian by Koolbye Formation, underlain by Hamersley Group.||||||
26271|Kungarra Formation|60706|5|Briefly described|p623 Fig.2|||Of the Turee Creek Group. Geological Province: Hamersley Basin||||||
26271|Kungarra Formation|62129|3|Fully described|p11|Archaean|Archaean|Of Turee Creek Group. Overlies conformably Boolgeeda Iron Formation, overlain confomably by Koolbye Formation. Thickness: 2800m. Geological Province: Hamersley Basin. Mudstone, siltstone and thin-bedded sandstone.||||||07-FEB-11
26271|Kungarra Formation|62130|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Turee Creek Group. Includes Meteorite Bore Member. Geological Province: Hamersley Basin, Pilbara Craton. Pelite and subordinate thin- to thick-bedded metasandstone.||||||23-MAR-09
26271|Kungarra Formation|64384|5|Briefly described|p37, p40|||Of Turee Creek Gp. Includes Meteorite Bore Member. Monotonous seq. of thin-bedded greyish-green siltstone, fine-gr.greywacke + fine-gr.sandstone; with thin carbonate beds in upper section; dolerite sills frequent. Unit overlain by seq. of quartz units||||||07-FEB-11
26271|Kungarra Formation|66574|4|Described|p914 Fig.3, p916 Fig.4|||Turee Creek Group. Underlies Koolbye Formation, overlies Boolgeeda Iron Formation. Upward-shallowing cycles of off-shore to prodelta turbiditic siltstone and mudstone;minor dolomitic sandstone and dolostone, dolerite sills. Includes Meteorite Bore Member.||||||
26271|Kungarra Formation|67130|5|Briefly described|p3 fig 2, p24 fig 17, p33 fig 28|||||Turee Creek Group|Includes Meteorite Bore Member|Overlies Boolgeeda Iron Formation, overlain by Koolbye Formation, Kazput Formation, Beasley River Quartzite|Sandstone and siltstone.|
26271|Kungarra Formation|67183|6|Mentioned|p645 Tb.1|Archean|Archean|Present in the Southern Pilbara.||Turee Creek Group||||
26271|Kungarra Formation|67201|5|Briefly described|p34 Fig.18|||||Turee Creek Group||||
26271|Kungarra Formation|68035|5|Briefly described|p292, Fig 6|Paleoproterozoic|Paleoproterozoic|Turee Creek Basin.||Of Turee Creek Group.|Includes Meteorite Bore Member.|Overlies Boolgeeda Iron Formation. Overlain by Koolbye Formation.|Sandstone, siltstone.|
26271|Kungarra Formation|68280|5|Briefly described|p5, p54-p57, p60|Paleoproterozoic|Paleoproterozoic|Wrongly called Kunganna formation once.||Turee Creek Group|Includes Meteorite Bore Member|Overlain by Koolbye Formation, overlies Boolgeeda Iron Formation|Sandstone and siltstone.|16-JAN-23
26271|Kungarra Formation|69003|5|Briefly described|p7-8|||Turee Creek Basin.||Turee Creek Group.|Meteorite Bore Member.|Overlies ?conformably the Boolgeeda Iron Formation. Is overlain ?conformably by Koolbye Formation.|Mostly deep-marine mudstones and turbidite sandstones, interbedded with minor dolostone.|
26271|Kungarra Formation|69028|5|Briefly described|Map Legend|Rhyacian|Siderian|Turee Creek Basin. Mapped with Koolbye and Kazput Formations as a single unit.|2445-2210 Ma|Of the Turee Creek Group.|||Mudstone, siltstone, sandstone, conglomerate, local stromatolitic dolomite, and basalt; metamorphosed.|07-MAY-14
26271|Kungarra Formation|69565|5|Briefly described|p131, p133 Fig.1, p140|||Hardey Syncline. Nearly 1000m thick. First mentioned as Kungarra shale.||Turee Creek Group.|Meteorite Bore Member.|Overlies Boolgeeda Iron Formation (Hamersley Group). Is overlain by Koolbye Formation.||
26271|Kungarra Formation|69754|4|Described|p314-p319, p322, p324, |Palaeoproterozoic|Palaeoproterozoic|Pilbara Craton. Age is derived from dates of the underlying Hamersley Group and the overlying Wyloo Group. ~1600m thick. Well exposed in the Hardey Syncline. Sedimentary facies are detailed. See also p329-p332, p336, p338-p341.||Turee Creek Group|Includes the Meteorite Bore Member.|Conformably overlies the Boolgeeda Iron Formation (Hamersley Group). Overlain by the Koolbye Formation. Unconformably overlain by the Cheela Springs Basalt.|Upwards fining succession of fine-grained sandstone, siltstone, and mudstone, in addition to coarse glaciogenic diamictites.|
26271|Kungarra Formation|70086|4|Described|p194-200,202-204,209|Paleoproterozoic|Siderian|Geological province: Pilbara Craton. Of the Hamersley Basin. Depositional environment: prodeltaic or mid-outer shelf environment. Minimum age constrained by U-Pb ages of detrital zircons in the Meteorite Bore Member (Takehara et al., 2010). Records a broadly shallowing-upward profile, from deepwater Booldeeda BIFs, to marine (Kungarra) to fluvial and shallow marine (Koolbye, Kazput) strata. Lithology described are a composite description from localities in the study, and does not necessarily representative of Kungarra Formation stratigraphy. Kungarra carbonates in the pre-glacial lower part of the Turee Creek Group formed during syndepositional or post-depositional diagenesis.|< ca. 2420 Ma|Unit of Turee Creek Group.|Includes Meteorite Bore Member.|Overlain by Koolbye Formation. Underlain by Boolgeeda Iron Formation/Hamersley Group.|Gray-green siltstone and shale, discontinuous limestone-bearing (stromatolitic) beds, occasional thin lenticular or planar beds of very fine- to fine-grained quartz-rich lithic arenites, coarsening upwards into very fine- to fine-grained sandstone.|
26271|Kungarra Formation|70795|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|West Australian Craton, Turee Creek Basin|2445-2208 Ma||||Pelite and subordinate thin to thickly bedded metasandstone; minor diamictite and dolerite sills.|
26271|Kungarra Formation|70958|4|Described|p2-3, Fig. 1|Paleoproterozoic|Paleoproterozoic|Type section locality in Beasley River area.||Of Turee Creek Group|Includes Meteorite Bore Member.|Appears to conformably overlie Boolgeeda BIF.|Laminated silty and flaggy shales in type area. Includes turbidites, diamictite, some basic volcanic flows and tuffs; a dolerite sill.|
26271|Kungarra Formation|71042|5|Briefly described|p66 fig 2|Paleoproterozoic|Paleoproterozoic|||Turee Creek Group||||
26271|Kungarra Formation|71112|5|Briefly described|p69,71,73-74,76,80|||Geological province: Pilbara Craton. Deposited between underfilled through to filled stages of the basin (where sedimentation rate < subsidence, then matched subsidence).|||Includes Meteorite Bore Member.|Overlain by Koolbye Formation. Underlain by Booldeega Iron Formation/Hamersley Group.|Shallowing-upward turbidite ramp and shallow-marine platform: siliciclastic sandstones and mudrocks, dolostones, glacial diamictites.|
26271|Kungarra Formation|71550|4|Described|p35-38,40-47|Siderian|Siderian|Geological province: Of Hamersley Basin. Depositional environment: Fine-grained siliciclastics. Includes a recently-discovered ca. 50 m-thick second diamictite located about 500m above the Meteorite Bore Member (Van Kranendonk and Mazumder, 2015). U-Pb zircon analyses of glacial diamictites, sandstone pebbles, a sandstone bar and a stromatolitic sample from this study yield maximum age of 2.34 Ga. Detrital provenance is likely from erosive products of underlyng Hamersley Province and Pilbara basement.||Unit of Turee Creek Group.|Includes the Meteorite Bore Member.|Basal unit of Turee Creek Group. Overlain by Koolbye Formation. Underlain by Boolgeeda Iron Formation/Hamersley Group.|Minor stromatolitic carbonates and glaciogenic strata.|03-SEP-19
26271|Kungarra Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Turee Creek Basin.||Turee Creek Group||Intruded by Balgara Dolerite sills.|Argillite and subordinate thin- to thick-bedded sandstone; local stromatolitic dolomite, diamictite, iron formation; intruded by Balgara Dolerite sills.|
26271|Kungarra Formation|72493|5|Briefly described|p30|||Hamersley Basin.||Basal Turee Creek Group.||Overlies Boolgeeda Iron Formation.|Epiclastic rocks.|
26271|Kungarra Formation|72570|5|Briefly described|p2|||||Turee Creek Group|Includes the Meteorite Bore  Member.|Conformably overlies the Boolgeeda Iron Formation. Overlain by the Koolbye Formation.|Upwards shallowing trend of siltstone, mudstone, symmetrically rippled and cross stratified sandstone and dolomitic sediments.|
26271|Kungarra Formation|72712|3|Fully described|p1, 6, 7, 9, p14-19, p23, 29, 43,44,49.|Rhyacian|Siderian|Originally defined by Trendall (1979) as the poorly exposed succession between the top of the Boolgeeda Iron Formation and the base of an unnamed ridge-forming quartzite. This formation is 2.8km thick in the Hardey Syncline. Various max. depositional ages determined from various parts of the Formation. Lowest horizon dated (c. 750m above base, 1250 m below Meteorite Bore Member) gave 2425+/-9 Ma U-Pb SHRIMP. Sample from c. 200m below Meteorite Bore Member gave 2406+/- 15 Ma. Maximum depositional ages from SHRIMP U-Pb detrital zircon studies suggest Woongarra Rhyolite and older units were the main source rock. Depositional age c. 2340 Ma. See also p36 Fig.25, p47, p50.|2208 +/- 10 Ma|Base of Turee Creek Group.|Meteorite Bore Member|Gradationally to disconformably overlies Boolgeeda Iron Formation. Partially underlies Anthiby Formation, Koolbye Formation. Intruded by Balgara Dolerite sills.|Mostly parallel laminated mudstone, parallel and ripple-laminated siltstone, normally graded quartz wacke, cross-stratified, fine-grained quartz arenite, dolomitic quartz arenite, dolomite (locally stromatolitic), and diamictite.|14-JAN-21
26271|Kungarra Formation|72758|6|Mentioned|p14 Tb.1.|||Mentioned only on p14 Tb.1.||||||
26271|Kungarra Formation|73538|5|Briefly described|p2 Fig. 1B, p3-5, App TbS1|Siderian|Siderian|A maximum age of 2340 +/- 22 Ma was reported by Caquineau et al. (2018).|Less than 2340 +/- 22 Ma|Turee Creek Group|Meteorite Bore Member|Underlain by Boolgeeda Iron Formation, Hamersley Group. Overlain by Koolbye Formation.|Siliciclastic sedimentary rocks, minor stromatolitic carbonates and two glaciogenic horizons.|
22146|Kunian Sandstone|14228|6|Mentioned|p6 fig3|Early Devonian|Early Devonian|North Canning Basin.||||||
22146|Kunian Sandstone|43563|6|Mentioned|p4|||||||||
22146|Kunian Sandstone|43803|2|Defined|p66||Ordovician|||||||
22146|Kunian Sandstone|50089|5|Briefly described|p430 Fig. 5|Ordovician|Ordovician|Geological Province: Canning Basin.||||||
22146|Kunian Sandstone|64334|5|Briefly described|p39-40|Ordovician|Ordovician|Eastern Lennard Shelf, Canning Basin. No outcrop. Tremadoc.||Prices Creek Group.||Is overlain by Kudata Dolomite.|Sandstone.|
22146|Kunian Sandstone|64580|6|Mentioned|map legend|||Of Prices Creek Group.||||||24-NOV-08
22146|Kunian Sandstone|64643|5|Briefly described|p6|||Of Prices Creek Group. No outcrop known. Intersected in mineral exploration drillholes and petroleum wells near the Emanuel Range.||||||24-NOV-08
22146|Kunian Sandstone|69099|5|Briefly described|500k_geologyp08_lut.csv|Middle Ordovician|Early Ordovician|||Prices Creek Group||||
22146|Kunian Sandstone|69165|6|Mentioned|500k_geologyp08_lut.csv|Ordovician|Ordovician|||Prices Creek Group||||
22146|Kunian Sandstone|69883|5|Briefly described|p4-p5|Arenig|Tremadocian|Canning Basin. Conodont zones and supersequences provided.||Prices Creek Group||Overlain by the Kudata Dolomite.|Transgressive sandstone.|
22146|Kunian Sandstone|71146|6|Mentioned|p26|||Canning Basin. ||Prices Creek Group||||
22146|Kunian Sandstone|71171|6|Mentioned|p1-p2, p5|||Canning Basin. Previously the lower Emanuel Formation.||Prices Creek Group||||
22146|Kunian Sandstone|73344|5|Briefly described|p3-4, p6, p12, p41, p51, p53, p62|Tremadocian|Tremadocian|Canning Basin, Lennard Shelf. Defined by Nicoll et al. (1993). Type section from 82 m, cores 4-6 from BMR Noonkanbah 3 well. Part of supersequence A0. Inferred as equivalent to coarse-clastic deposits in the Fly Flat Member of the Nambeet Formation. Does not contain any fossil material.||Prices Creek Group||Overlain by Kudata Dolomite. Equivalent to Fly Flat Member (Nambeet Formation) and Wilson Cliffs Sandstone.|Quartz-lithic arenite with occasional glauconite-rich units throughout.|
25981|Kuniandi Group|22496|6|Mentioned|p10, p11|||On MOUNT RAMSAY sheet.  Contains the Landrigan Tillite which correlates with the Moonlight Valley Tillite.  Correlated with the Duerdin Group.||||||16-AUG-04
25981|Kuniandi Group|22547|6|Mentioned|p28|||Correlates with Duerdin Group||||||
25981|Kuniandi Group|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
25981|Kuniandi Group|22764|5|Briefly described|Table1,p6||Adelaidean|||||||01-FEB-10
25981|Kuniandi Group|23383|5|Briefly described|p20|||Disconformably overlain by the Louisa Downs Group.  Correlated with Mount House Group and Duerdin Group by Plumb (1996).||||||25-JAN-05
25981|Kuniandi Group|23516|6|Mentioned|p599 Fig.6|||||||||
25981|Kuniandi Group|23599|5|Briefly described|p17|Neoproterozoic|Neoproterozoic|Overlying unit Louisa Downs Group||||||
25981|Kuniandi Group|23621|6|Mentioned|p32|||||||||
25981|Kuniandi Group|23806|5|Briefly described|p1122|Neoproterozoic|Neoproterozoic|Max. thickness: 100m.||||||
25981|Kuniandi Group|24173|5|Briefly described|p24|Neoproterozoic|Neoproterozoic|Geological Province: Wolfe Basin. In the MOUNT RAMSAY 1:250,000 sheet area. Correlates with Duerdin Group.||||||09-DEC-08
25981|Kuniandi Group|30097|6|Mentioned|Table 23|||See also Table 24,25 and Fig.54||||||
25981|Kuniandi Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
25981|Kuniandi Group|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
25981|Kuniandi Group|31393|6|Mentioned|Pl.25|||||||||
25981|Kuniandi Group|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
25981|Kuniandi Group|32660|4|Described|Table 6|||||||||
25981|Kuniandi Group|32728|6|Mentioned|Fig.3|||||||||
25981|Kuniandi Group|35120|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
25981|Kuniandi Group|36551|6|Mentioned|Table 10|||See also p48.||||||27-MAY-15
25981|Kuniandi Group|36888|4|Described|p215|||||||||
25981|Kuniandi Group|36898|6|Mentioned|p188|||||||||
25981|Kuniandi Group|37299|6|Mentioned|Fig.1|||||||||
25981|Kuniandi Group|37462|4|Described|Table 4.X|||||||||
25981|Kuniandi Group|37927|6|Mentioned|p504|||||||||
25981|Kuniandi Group|38157|6|Mentioned|Table X|||||||||
25981|Kuniandi Group|38988|6|Mentioned|Fig.4|||||||||
25981|Kuniandi Group|40105|6|Mentioned|p313|||||||||
25981|Kuniandi Group|42811|6|Mentioned|p30|||||||||
25981|Kuniandi Group|43281|5|Briefly described|Map legend||Proterozoic|||||||
25981|Kuniandi Group|43595|6|Mentioned|p550|||||||||
25981|Kuniandi Group|43666|6|Mentioned|p51,Table 2||Neoproterozoic|||||||
25981|Kuniandi Group|44140|5|Briefly described|p299, p300, p301 fig 4-7|Neoproterozoic|Neoproterozoic|Correlated with Sturtian glaciation (750 Ma). Of Mount Ramsay area.|c.750 Ma.||Includes Landrigan Tillite, Stein and Wirara Formations, and Mount Bertram Sandstone.|Overlain unconformably by Louisa Downs Group.|Basal diamictite overlain by a thin persistent dolomite unit that passes up into thick sequences of mostly green or grey siltstone, shale and sandstone; glacial deposits; locally derived.|07-MAR-18
25981|Kuniandi Group|44155|6|Mentioned|p250-251, p254 Fig.3-40|Neoproterozoic|Neoproterozoic|Glacial sequence. Appears as Kundiandi Group in Fig.3-40.||||||
25981|Kuniandi Group|44231|5|Briefly described|Map Legend|Neoproterozoic III|Neoproterozoic III|Includes the Landrigan Tillite, Stein and Wirara Formations, and Mount Bertram Sandstone. Age: c.610Ma. Geological Province: Louisa Basin.||||||26-MAY-05
25981|Kuniandi Group|44366|14|Not recorded|p.17|||||||||
25981|Kuniandi Group|44397|14|Not recorded|p.15,19,Fig.4,Table3||Adelaidean|See p.6,10,16.||||||
25981|Kuniandi Group|44398|14|Not recorded|map legend||Adelaidean|||||||
25981|Kuniandi Group|45047|6|Mentioned|p36|||Table. Adelaidean.||||||
25981|Kuniandi Group|45140|6|Mentioned|p13|||Kimberley region.|~700 Ma.|||||
25981|Kuniandi Group|48927|2|Defined|p10|Adelaidean|Adelaidean|||||||
25981|Kuniandi Group|60724|6|Mentioned|p5 Fig. 2|Neoproterozoic|Neoproterozoic|||||||
25981|Kuniandi Group|63458|6|Mentioned|p872 Fig.1, p873 Fig.2, p874. |Ediacaran|Cryogenian|Mount Ramsay area, Kimberley region. See also p880 Fig.6, p882 Fig.8, p891, p897 Fig.19.|||Includes Landrigan Tillite; Stein, Wirara Formations; Mount Bertram Sandstone.|||
25981|Kuniandi Group|64104|6|Mentioned|p70 fig 7|Neoproterozoic|Neoproterozoic|||||||
25981|Kuniandi Group|64580|4|Described|map legend||Ediacaran|Siltstone, sandstone, shale, feldspathic wacke, dolomite, and tillite.||||||09-DEC-08
25981|Kuniandi Group|67484|6|Mentioned|p294 Tb.1|Ediacaran|Cryogenian|Mount Ramsay area, West Kimberley. |||Includes Mount Bertram Sandstone; Wirara, Stein and Landrigan Formations.|Overlain by the Louisa Downs Group.||27-MAY-15
25981|Kuniandi Group|67620|5|Briefly described|p2-3, 5|Ediacaran|Cryogenian|Mount Ramsay area, Kimberley region.|||Landrigan, Stein, Wirara Formations; Mount Bertram Sandstone.|Is overlain by Louisa Downs Group.||
25981|Kuniandi Group|68138|6|Mentioned|p154, 156|Neoproterozoic|Neoproterozoic||||Landrigan, Stein, Wirara Formations; Mount Bertram Sandstone.|||
25981|Kuniandi Group|68244|4|Described|p659-660,662-666|Neoproterozoic|Neoproterozoic|Louisa Basin, Kimberley region. ~1000m thick. Outcrops on the eastern limb of Louisa Syncline and upturned limbs of the west-east-oriented McKinnon Syncline.|||Includes Mount Bertram Sandstone, Wirara Formation, Stein Formation and Landrigan Formation.|Overlain unconformably by Louisa Downs Group. Underlain unconformably by Kimberley Group, Halls Creek Group and Lamboo Complex.||
25981|Kuniandi Group|68473|6|Mentioned|p530-p531|Neoproterozoic|Neoproterozoic|Kimberley region.|||Includes the Landrigan Tillite, Stein Formation, Wirara Formation, Mt Bertram Sandstone.|||
25981|Kuniandi Group|69003|6|Mentioned|p5|||Halls Creek Orogen.||||||
25981|Kuniandi Group|69099|5|Briefly described|500k_geologyp08_lut.csv||||||||Siltstone, sandstone, shale, feldspathic wacke, dolomite, and tillite.|31-JUL-15
25981|Kuniandi Group|69165|4|Described|500k_geologyp08_lut.csv|Ediacaran|Ediacaran||||||Undivided; siltstone, sandstone, shale, feldspathic wacke, dolomite and tillite.|
25981|Kuniandi Group|69597|6|Mentioned|p5 fig 2b|||||||||
25981|Kuniandi Group|69634|5|Briefly described|500k_geologyp08_lut.csv||Ediacaran||||||Undivided; siltstone, sandstone, shale, feldspathic wacke, dolomite, and tillite|
25981|Kuniandi Group|70154|4|Described|500k_interpgeop14_lut.csv|Ediacaran|Cryogenian||541-850 Ma||||Siltstone, sandstone, shale, feldspathic wacke, dolomite and tillite|
25981|Kuniandi Group|70731|6|Mentioned|p268|Neoproterozoic|Neoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.||||||
25981|Kuniandi Group|70826|6|Mentioned|p5 tbl 2|||Supersequence 3, Centralian Superbasin.||||||20-APR-20
25981|Kuniandi Group|71267|4|Described|GEOL_LUT_CSV files|Ediacaran|Cryogenian|Of Louisa Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|720-541 Ma (inferred)||Includes Bulka Hills Beds, Kai Ki Beds, Landrigan Tillite, Mount Bertram Sandstone, Stein Formation, Wade Creek Sandstone, Wirara Formation.||Siltstone, sandstone, shale, feldspathic wacke, dolomite, and tillite.|
25981|Kuniandi Group|72034|5|Briefly described|500k_interpgeop16_lut|Ediacaran|Cryogenian|Louisa Basin.|||||Siltstone, sandstone, shale, feldspathic wacke, dolomite, and tillite.|
74752|Kunmarnara Group|65135|4|Described|p1, p16|Stenian||New unit name. Of Bentley Supergroup. Originally part of Tollu Group. Redefined in this paper to include MacDougall Formation and Mummawarrawarra Basalt. Unconformably underlies redefined Tollu Group. Maximum age is poorly constrained, but must be older than ~1078. An age gap of potentially more than 50 myr separates Kunmarnara Group from overlying Tollu Group.||||||16-JAN-15
74752|Kunmarnara Group|65693|6|Mentioned|p3 Fig.1.|||||||||
74752|Kunmarnara Group|65833|5|Briefly described|p1, p6 Fig.4, p16|Stenian|Stenian|Of Bentley Supergroup. Overlain by Tollu Group. Some components of old Tollu Group (layered mafic-ultramafic intrusions)- MacDougall Formation and Mummawarrawarra Basalt - have been reassigned in this paper to Kunmarnara Group, because they are cut by feeder dykes for volcanic units in the overlying Tollu Group. Age >1078 Ma.||||||
74752|Kunmarnara Group|65898|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of Bentley Supergroup, Bentley Basin. Age shown as >1078 Ma. Includes Macdougall Formation. ||||||
74752|Kunmarnara Group|65906|6|Mentioned|p19|Mesoproterozoic|Mesoproterozoic|Volcanic rocks. Intruded by the Giles Complex. Age: ~1172 Ma. Repeatedly mis-spelt as Kunmanara on p19-20.||||||
74752|Kunmarnara Group|66280|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Age shown as >1078 Ma. Shown as the only unit in Bentley Supergroup in this map area. Includes MacDougall Formation and a unit of unassigned metasiliciclastic and metamafic volcanic rocks.||||||
74752|Kunmarnara Group|66281|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|>1078 Ma.|Unit in Bentley Supergroup.|Includes MacDougall Formation and Mummawarrawarra Basalt.||Siliciclastic and mafic volcanic rocks.|
74752|Kunmarnara Group|66282|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|>1078 Ma.|Unit in Bentley Supergroup.|Includes Mummawarrawarra Basalt and MacDougall Formation.|||
74752|Kunmarnara Group|67128|4|Described|p5 Fig.3,p7,p11 p15,p18-19,p27,p31-33|||Smithies et al. (2009); formerly the basal rift succession of the Tollu Group of Daniels (1974). Mainly exposed along the NE boundary of the Mamutjarra Zone, western Musgrave Province. Age is constrained by youngest detrital zircons of the MacDougall Formation (c.1172 Ma), and a 1078 +/- 3 Ma intrusion.|c.1100 Ma.|Bentley Supergroup.|MacDougall Formation, Mummawarrawarra Basalt.|Is overlain by Townsend Quartzite.|Typical intracontinental rift sequence: basal conglomerates and sandstones followed by basalt flows.|
74752|Kunmarnara Group|67244|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Unit in Bentley Supergroup.|Includes MacDougall Formation and Mummawarrawarra Basalt.|||
74752|Kunmarnara Group|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. ||Unit in Bentley Supergroup.|Includes MacDougall and Skirmish Hill Formations and Mummawarrawarra Basalt.||Volcanic and volcaniclastic rocks; quartz-pebble conglomerate and sandstone.|
74752|Kunmarnara Group|67375|2|Defined|pp8-9 Fig.5, pp40-4, p63, pp216-228.|Mesoproterozoic|Mesoproterozoic|Defined to include the lower two units of the former Tollu Group which are cut by Giles Suite intrusions, whereas the younger units are clearly younger than the Giles Suite. A typical intracontinental rift sequence; undivided siliciclastic and mafic volcanic rocks; the Group traces the rift-basin boundaries. Outcrops mainly along the southwestern boundary of the NW-trending Tjuni Purlka Tectonic Zone. Named after Kunmarnara Bore, 4 km east of MacDougall Bluff. Tentatively correlated with lower units of the Tjauwata Group in NT, but may pre-date that Group.|1172 +/- 8 Ma - 1076 +/- 7 Ma.|Unit in Bentley Supergroup.|Includes MacDougall Formation and Mummawarrawarra Basalt.|Unconformably overlies Wankanki Supersuite. Is intruded by Giles Suite. Is overlain unconformably by Tollu Group.|Sequence of basal conglomerates and sandstones, followed by basalt flows.|30-OCT-12
74752|Kunmarnara Group|67553|4|Described|p8,11,17,35,37,39-40,42,55,p59,84|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Depositional age at 1078+\-4 Ma. Emplacement of mafic-ultramafic Giles intrusions within Kunmarnara Group, prior to Tollu Group deposition. Occurs in the SE and central part of Musgrave province. Represents the basal succession of the Ngaanyatjarra Rift (Evins et al., 2010). The rift splits into a NW trending northern arm and a SW trending southern arm.|c. 1078 Ma|Unit of Warakurna Supersuite and Bentley Supergroup.|Includes MacDougall Formation and Mummawarrawarra Basalt.|Overlain unconformably by Tollu Group.||06-AUG-19
74752|Kunmarnara Group|67888|6|Mentioned|p65|||Oldest unit of the Bentley Supergroup.||Bentley Supergroup||||
74752|Kunmarnara Group|68100|6|Mentioned|p2, 3, 5, 8|||||Bentley Supergroup|Includes MacDougall Formation, Mummawarrawarra Basalt|Intruded/overlain by Warakurna Supersuite||
74752|Kunmarnara Group|68995|5|Briefly described|p1, p3-7, p47, p64|||||Bentley Supergroup|MacDougall Formation, Mummawarrawarra Basalt|Unconformably overlies the Wirku Metamorphics and the Pitjantjatjara Supersuite.|Basalt, granofels and metasandstone.|
74752|Kunmarnara Group|68996|5|Briefly described|p4, 7, 26, 28-30, 41, 43,45,47,63,65,68|Mesoproterozoic|Mesoproterozoic|May be conductive. Unit relationships show this Group older than Giles Suite rocks. Shows isoclinal folding. Misspelt Kurnmarnara Group p29.||Base of Bentley Supergroup|Includes Skirmish Hill Volcanics|Intruded by mafic-ultramafic rocks of Giles Suite.|Dominantly amygdaloidal basalts, metabasalts and quartz pebble conglomerates. Also rhyolitic to dacitic volcanics. Density values range from 2.63-3.19g/cm^3.|
74752|Kunmarnara Group|69003|5|Briefly described|p37, p50|Mesoproterozoic|Mesoproterozoic|Blackstone Sub-basin, W Musgrave Province. Represents the basal succession of the Ngaanyatjarra Rift.||Bentley Supergroup.||Is intruded by the Giles intrusions.||
74752|Kunmarnara Group|69009|5|Briefly described|Map Legend|Stenian|Stenian|Bentley Basin.|c. 1078 Ma|Of the Bentley Supergroup.|Includes MacDougall Formation.||Undivided siliciclastic and mafic volcanic rocks.|04-APR-14
74752|Kunmarnara Group|69091|4|Described|p52 Fig.4.1, p56, see comments|||Overlies northern parts of west Musgrave Province. Magnetic anomalies highlight intensely folded region correlating with Kunmarnara Group south of Woodroffe Thrust. Misspelled as Kunmarna Group on p117 Fig.5.15. See also p59 Fig.4.6, p70-73, p76, p80, p82-84, p86-87, p103 Fig.5.6, p105-107, p109 Fig.5.10, p115 Fig.5.14, p117 Fig.5.15, p131-132, p134 Fig.6.2, p142, p144.||Basal Bentley Supergroup.|Mummawarrawarra Basalt (upper part), MacDougall Formation (at base)|Equivalent to Tjauwata Group; unconformably overlies Pitjantjatjara Supersuite, Wankanki Supersuite, Wirku Metamorphics.|Quartz sandstones, pebbly sandstones and conglomerates (MacDougall Formation), basalts (Mummawarrawarra Basalt), and minor felsic volcanic rocks; granofels and metasandstone.|26-SEP-14
74752|Kunmarnara Group|69153|5|Briefly described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen||Bentley Supergroup|Skirmish Hill Formation, Mummawarrawarra Basalt, MacDougall Formation (lowermost unit in group)||Metasiliciclastic and metamafic volcanic rocks|
74752|Kunmarnara Group|69436|5|Briefly described|p21:14|||The MacDougall Formation and Mummawarrawarra Basalt, hitherto of the Tollu Group, are now reassigned to the Kunmarnara Group, which is regarded as the basal succession of the Bentley Supergroup.||Basal Bentley Supergroup.|MacDougall Formation, Mummawarrawarra Basalt.|Is overlain unconformably by the (redefined) Tollu Group.||12-JUL-16
74752|Kunmarnara Group|69655|5|Briefly described|p3, p6, p33-p35, p59, p62, p77-p78|Stenian|Stenian|Musgrave Region.|c. 1090-1040 Ma|Bentley Supergroup||Intruded by the Alcurra Dolerite suite.||
74752|Kunmarnara Group|69729|5|Briefly described|p66 Fig.1,p67-68 p70,p79-80,p82,p86-87|||Bentley Basin. Post-dates Musgrave Orogeny metamorphism at c.1120 Ma, and pre-dates intrusions at c.1090 Ma and c.1078 Ma.||Bentley Supergroup.|MacDougall Formation, Mummawarrawarra Basalt.||A succession of quartz sandstones, pebbly sandstones, and conglomerates, basalts and minor felsic volcanic rocks.|
74752|Kunmarnara Group|70095|5|Briefly described|p17|||Geological province: Musgrave Province. Of Talbot Sub-basin, Bentley Basin.||||Overlain by Giles intrusions or Winburn granite or Mount Palgrave Group.|Granofels and metasandstone.|
74752|Kunmarnara Group|70134|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Bentley Supergroup.|MacDougall Formation.|||
74752|Kunmarnara Group|70619|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Bentley Supergroup.|Mummawarrawarra Basalt, MacDougall Formation|||03-JUN-16
74752|Kunmarnara Group|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|SHRIMP date from a syenite (file 183847.1.pdf) |1075 Ma - 1085 Ma, 1078 Ma +/- 4 Ma (SHRIMP)|Bentley Supergroup|Includes MacDougall Formation||Unassigned metasiliciclastic and metamorphosed mafic volcanic rocks; minor felsic volcanic rocks.|
74752|Kunmarnara Group|70763|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Nine facies, two of which are named, are mapped separately.||Bentley Supergroup.|MacDougall Formation, Mummawarrawarra Basalt.|||
74752|Kunmarnara Group|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Forms the basal succession of the Ngaanyatjarra Rift (Evins et al., 2010). Deposited unconformably over Mesoproterozoic rocks of the Musgrave Province along the WNW basin margin of the Ngaannyatjarra Rift (intracontinental rift-type). Principal outcrop of the Bentley Supergroup in the west Musgrave region. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Sample GSWA 183847 (syenite; also by definition part of Warakurna Supersuite) yielded an interpreted (regression intersecting concordia) magmatic crystallisation age of 1078+\-4 Ma. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeol_lut.csv.|1085-1075 Ma (inferred)|Unit of Bentley Supergroup.|Includes MacDougall Formation, Mummawarrawarra Basalt, Skirmish Hill Formation.||Undivided siliciclastic and mafic volcanic rocks; minor felsic volcanic rocks; metamorphosed.|
74752|Kunmarnara Group|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Bentley Basin. ||Bentley Supergroup||||
74752|Kunmarnara Group|70831|5|Briefly described|p1-p2, p4-p6, p9, p20-p22|Stenian|Stenian|Bentley Basin. Deposited during the Giles Event.|c. 1085-1040 Ma|Bentley Supergroup|Includes the MacDougall Formation and the Mummawarrawarra Basalt.|||
74752|Kunmarnara Group|70839|5|Briefly described|p326-327|||Geological province: Musgrave Province. Of Bentley Basin. Primarily a unit of Warakurna Supersuite, however volcanic components are also part of Bentley Supergroup. Emplaced within, and the basal unit of Ngaanyatjarra Rift (Evins et al., 2010; Aitken et al., 2012). Dominated by c. 1.2 Ga detrital zircons reworked from Musgrave Orogen, smaller 1.63-1.50 Ga detrital components.||Unit of Warakurna Supersuite and Bentley Supergroup.||||
74752|Kunmarnara Group|71088|5|Briefly described|p4-p6|||Bentley Basin. Deposited within the structural Ngaanyatjarra Rift.||Bentley Supergroup||Overlain by and interbedded with the Warakurna Supersuite. Equivalent to the Tjauwata Group.||
74752|Kunmarnara Group|71170|5|Briefly described|p5-p6|||Emplaced during the Giles Event.||||||
74752|Kunmarnara Group|71210|5|Briefly described|p4-p5, p8-p9, p21-p22|||Blackstone and Talbot Sub-basins. See also p51-p52, p79, p113, p136.||Bentley Supergroup|Includes the MacDougall Formation and the Mummawarrawarra Basalt.|Overlies the Pitjantjatjara Supergroup.||
74752|Kunmarnara Group|71211|5|Briefly described|p6, p7 fig 1.4, p24 fig 2.1|||See also p84 fig 3.1. p136 fig 4.1, p216, p233. ||Bentley Supergroup|Includes the MacDougall Formation and the Mummawarrawarra Basalt.||Granofels and metasandstone.|
74752|Kunmarnara Group|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Deposited unconformably over Mesoproterozoic rocks of the Musgrave Province along the W to WNW trending margins of the Ngaannyatjarra Rift. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogen (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Sample GSWA 183471 (syenite) yielded a regression line crossing concordia curve at 1078+\-4 Ma, interpreted as the magmatic crystallization age of the syenite. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeol_lut.csv.|1085-1075 Ma (inferred)|Unit of Bentley Supergroup.|Includes MacDougall Formation, Mummawarrawarra Basalt, Skirmish Hill Formation.||Unassigned metamorphosed siliciclastic and mafic volcanic rocks|
74752|Kunmarnara Group|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1078+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Syenite, quartzite.|
74752|Kunmarnara Group|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Bentley Supergroup|Includes Skirmish Hill Formation, MacDougall Formation||Undivided siliciclastic and mafic volcanic rocks; minor felsic volcanic rocks. Unassigned metamorphosed siliciclastic and mafic volcanic rocks.|
74752|Kunmarnara Group|72094|4|Described|p2, 3, p4-7, 11, 12, 13, 14, p15-16, 17|Stenian|Stenian|Bentley Basin. Siliciclastics sediments deposited and mafic extrusive magmas within the Bentley Basin associated with Giles Event Stage 1. Syenitic volcanic rock dated at 1078+/-4 Ma, and leucogabbrio intrusion dated at 1076+/-7 Ma provide minimum depositional age.|1085-1075 Ma|Unit of Bentley Supergroup.|Inclues MacDougall Formation|Tectonically interleaved with Warlawurru Supersuite and Pitjantjatjara Supersuite. Unconformably overlain by Cobb Embayment sediments. Equivalent to Tjauwata Group.|Siliciclastic sediments and mafic magmas. Paragneiss.|
74752|Kunmarnara Group|72443|5|Briefly described|p737-739|||Bentley Basin. Remnants are preserved over an area that suggests a once continuous depositional basin of >50000km^2.||Bentley Supergroup|||Medium- to coarse-grained siliciclastic rocks and basalt flows.|
74752|Kunmarnara Group|73437|5|Briefly described|p151, p155|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Age of peak metamorphism indicated by U-Pb dates of 631+/-12 Ma and 628+/-4 Ma for metamorphic rims on detrital zircons, from northern hinterland area around Mikita.||Bentley Supergroup|MacDougall Formation, Mummawarrawarra Basalt||Includes metasediments.|
40772|Kurrajong Complex|24494|5|Briefly described|p17|||Differentiated komatiite unit. Geological Province: Eastern Goldfields Granite-Greenstone Terrane, Yilgarn Craton.||||||
75854|Kurrajong Monzogranite|64775|6|Mentioned|p16-1, 18-1|||||||||
26677|Kurrawang Formation|22534|5|Briefly described|p21, Fig.3 p6||Archean|See also Fig.4 p7, Table 2 p8||||||07-NOV-08
26677|Kurrawang Formation|22539|5|Briefly described|Map legend|Archean|Archean|||||||07-NOV-08
26677|Kurrawang Formation|22596|6|Mentioned|Fig.9 p419|||||||||
26677|Kurrawang Formation|22682|5|Briefly described|p14|||Kurrawang Supersequence||||||
26677|Kurrawang Formation|23141|6|Mentioned|p216|||||||||
26677|Kurrawang Formation|23281|6|Mentioned|p5|||||||||
26677|Kurrawang Formation|23584|6|Mentioned|p10|||||||||
26677|Kurrawang Formation|23595|6|Mentioned|p18|||||||||
26677|Kurrawang Formation|23928|5|Briefly described|p64|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
26677|Kurrawang Formation|24139|5|Briefly described|p239 Table 1|||Geological Province: Ora Banda Domain.||||||
26677|Kurrawang Formation|24174|5|Briefly described|p39|Archean|Archean|Geological Province: Eastern Goldfields.||||||07-NOV-08
26677|Kurrawang Formation|24196|5|Briefly described|p47 Fig.5|Archean|Archean|Age: <2679 +/- 10 Ma. Geological Province: Kalgoorlie Terrane, Yilgarn Craton.||||||07-NOV-08
26677|Kurrawang Formation|24305|5|Briefly described|p919|||||||||
26677|Kurrawang Formation|39869|6|Mentioned|p352|||||||||
26677|Kurrawang Formation|42221|5|Briefly described|p11|||||||||
26677|Kurrawang Formation|42382|5|Briefly described|Fig.9 P49|||||||||
26677|Kurrawang Formation|42436|5|Briefly described|p73|||||||||
26677|Kurrawang Formation|42696|6|Mentioned|Plate 1B|Archean||||||||07-NOV-08
26677|Kurrawang Formation|42705|5|Briefly described|map legend|Archean||||||||07-NOV-08
26677|Kurrawang Formation|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
26677|Kurrawang Formation|42870|5|Briefly described|Table 1, P67|||||||||
26677|Kurrawang Formation|42892|4|Described|p28|||||||||
26677|Kurrawang Formation|42988|5|Briefly described|Map Legend|||||||||
26677|Kurrawang Formation|42989|5|Briefly described|p11|||||||||
26677|Kurrawang Formation|43101|5|Briefly described|Table 1.|||||||||
26677|Kurrawang Formation|43162|6|Mentioned|5|||||||||
26677|Kurrawang Formation|43214|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
26677|Kurrawang Formation|43232|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
26677|Kurrawang Formation|43496|6|Mentioned|6,15|||||||||
26677|Kurrawang Formation|44149|5|Briefly described|p85 Tb.2-8, p88, p91 Tb.2-9|Archean|Archean|See also p108 Fig.2-117, p109. Eastern Goldfields Province. Appears as Kurrawang Conglomerate on p85.|||||Conglomerate, sandstone.|
26677|Kurrawang Formation|46311|14|Not recorded|Map Legend.|||||||||
26677|Kurrawang Formation|50421|4|Described|p285||Archean|<2655 Ma. Quarztofeldspathic turbidite beds. Unconformably overlies Black Flag Group. One of the uppermost units of the Kalgoorlie Terrane.||||||07-NOV-08
26677|Kurrawang Formation|60076|5|Briefly described|p12 Tb. 2, p21|Archean|Archean|See also Karrawang Fm. Polymictic conglomerate with high content of BIF clasts; sst. and sltst.  Unconformably overlies Black Flag Gp.  Max. thick: 750m conglom. + 1300m sst/sltst.  Geol.Prov: Ora Banda domain (Yilgarn Craton). See also p27, p45 App.1.||||||07-NOV-08
26677|Kurrawang Formation|60514|6|Mentioned|p33, p62|Archean|Archean|Consists of graphitic black shale, intermediate volcaniclastic rocks, dolerite sills, and polymictic conglomerate. Geological Province: Yilgarn Craton.||||||07-FEB-11
26677|Kurrawang Formation|60555|5|Briefly described|p12|Archean|Archean|Age: 2671+/-3Ma and 2679+/-10Ma (Krapez et al., 2000. Detrital zircons).||||||30-NOV-09
26677|Kurrawang Formation|60623|5|Briefly described|p33|Archean|Archean|Turbidite fan deposit.||||||07-NOV-08
26677|Kurrawang Formation|60627|5|Briefly described|p62, p65 Tb.1|||Polymictic conglomerate, immature sandstone with coarse trough cross beds, graded beds.||||||
26677|Kurrawang Formation|62097|6|Mentioned|p310|Archean|Archean|Geological Province: Kalgoorlie Terrane in Eastern Godlfields Superterrane of the Yilgarn Craton.||||||07-NOV-08
26677|Kurrawang Formation|64633|6|Mentioned|p4 Fig.3, p6 Fig.4, p8.|||?Kalgoorlie Terrane or later basin?|<2679 +/- 10 (Krapez et al. 2000).|||||24-APR-17
26677|Kurrawang Formation|64715|5|Briefly described|p1, p3|||Represents the Black Flag Group about 10km west of Mount Hunt.||||||16-DEC-08
26677|Kurrawang Formation|65204|5|Briefly described|pg6 Tbl.1, p13, p15, p16||Neoarchean|Sandstone and conglomerate foramtion; contains cross beds and graded beds; divided into lower unit of polymictic  matrix-supported conglomerate and upper unit of medium-coarse grained lithic sandstone; unconformably overlies Black Flag Group; may be up to 2000m thick.||||||
26677|Kurrawang Formation|65262|6|Mentioned|p4, p8|Archean|Archean|Yilgarn Craton.|||||Metamorphosed sedimentary rocks.|
26677|Kurrawang Formation|65264|6|Mentioned|p13, p19, p20|Archean|Archean|Unconformably overlies Black Flag Group. Age: <2655Ma. Consists of medium- to coarse-grained, locally pebbly, lithic sandstone in upper section;  BIF is present as the dominant clast type in the conglomeratic unit. See also p21, p51 Appdx. 1||||||07-FEB-11
26677|Kurrawang Formation|65834|6|Mentioned|p7|||Ora Banda Domain, Kalgoorlie Terrane.|||||Polymictic conglomerate; immature sandstone. Coarse trough cross-beds, graded beds.|
26677|Kurrawang Formation|66880|6|Mentioned|p8 Fig.2. |Archean|Archean||2679 +/- 10 Ma (Krapez et al. 2000).|||||
26677|Kurrawang Formation|67198|5|Briefly described|p5 fig 2|Neoarchean|Neoarchean|Kalgoorlie Terrane, Late Basins. Ages derived from sandstones.|<2679 +/-10 Ma, <2657 +/- 4 Ma||||Sedimentary rocks, mainly coarse conglomerate.|11-SEP-17
26677|Kurrawang Formation|68289|5|Briefly described|p7, p11, p16|||Southern Kalgoorlie Terrane. Represents the "late basin" sediments in this area. Outcrop localities provided.|||||Sedimentary rocks including polymictic conglomerate with clasts of banded-iron formation and granite.|
26677|Kurrawang Formation|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton|||Includes 3 unnamed subunits.||Lower units: conglomerate, sandy conglomerate, and pebbly sandstone; conglomerate with banded iron-formation clasts (magnetic horizon); metamorphosed. Upper unit: sandstone and pebbly sandstone; metamorphosed|
26677|Kurrawang Formation|69404|5|Briefly described|p4|Neoarchean|Neoarchean|Overlies all greenstones in the Eastern Goldfields Superterrane.|2658-2655 Ma||||Polymictic conglomerate and sandstones.|
26677|Kurrawang Formation|69583|5|Briefly described|p37|||Contains a variety of clasts (including BIF and granite) indicating a distal provenance, probably in the Youanmi Terrane.|||||Polymictic conglomerate.|
26677|Kurrawang Formation|69631|5|Briefly described|p7, p11, p18|Neoarchean|Neoarchean|Southern Kalgoorlie Terrane. Late basin sediments: possibly a submarine fan deposit. The nature of clasts indicates a distal provenance, possibly in the Youanmi Terrane. Geochronology by Kositcin et al. (2008).|<2655 Ma (maximum depositional age).|||Unconformably overlies Navajo Sandstone.|Coarse, poorly sorted polymictic conglomerate; a variety of clasts including BIF and granite. Grades up into fine-grained sandstone and siltstone.|
26677|Kurrawang Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|See also 500k_interpgeop14_lut.csv and 100k_geologyl10_lut.csv.|2657 - 2640 Ma (inferred).||Includes Seven Mile Sandstone, Lake Douglas Conglomerate||Lower unit: conglomerate with clasts of banded iron-formation (magnetic horizon), granite, quartzite and mafic volcanics; metamorphosed. Upper unit: sandstone and pebbly sandstone; metamorphosed.|
26677|Kurrawang Formation|70156|4|Described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Youanmi Terrane events (3200-2600 Ma).|2657-2640 Ma (inferred)||||Conglomerate, sandy conglomerate, pebbly sandstone to sandstone; polymictic with clasts of banded iron-formation, granite, quartzite and mafic volcanic; planar- and cross-bedding; metamorphosed|
26677|Kurrawang Formation|70482|6|Mentioned|p318|Archean|Archean|W of Kalgoorlie, Yilgarn Craton. Intra-arc to backarc environment.||||||
26677|Kurrawang Formation|70773|6|Mentioned|p18 fig 11, p21|||||||||
26677|Kurrawang Formation|70794|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton. Also 2_5m_interpgeop15_lut.csv.|2657-2640 Ma inferred||||Conglomerate, sandy conglomerate, pebbly sandstone to sandstone; polymictic with clasts of banded iron formation, granite, quartzite and mafic volcanics; planar- and cross-bedding; metamorphosed.|
26677|Kurrawang Formation|70826|6|Mentioned|p9|Neoarchean|Neoarchean|||||||13-MAY-20
26677|Kurrawang Formation|71148|6|Mentioned|p123|||Nimbus mine area, c.10km E of Kalgoorlie.|||||Conglomerate.|
26677|Kurrawang Formation|71212|4|Described|p241|Neoarchean|Neoarchean|Kalgoorlie region. Deposited as high-density, coarse-grained and low-density, fine-grained turbidites on a submarine fan. |Approx. 2660 Ma.|||Unconformably overlies the Black Flag Formation.|Upwards fining succession of quartzofeldspathic conglomerate, sandstone and mudstone.|
26677|Kurrawang Formation|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 100k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv, 100k_geologyl10_lut.csv.|||Includes Lake Douglas Conglomerate, Seven Mile Sandstone.||Lower unit: conglomerate with banded iron-formation clasts (magnetic horizon) and sandy conglomerate and pebly sandstone; metamorphosed. Upper unit: sandstone and pebbly sandstone; metamorphosed.|
26677|Kurrawang Formation|71308|5|Briefly described|p711 Fig.2|||Kalgoorlie Terrane.|<2660 Ma.||||Sedimentary rocks.|
26677|Kurrawang Formation|71309|6|Mentioned|p740 Fig.3|||||||||
26677|Kurrawang Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||||||Conglomerate, sandy conglomerate, pebbly sandstone to sandstone; polymictic with clasts of banded iron-formation, granite, quartzite and mafic volcanic; planar- and cross-bedding; metamorphosed.|
26677|Kurrawang Formation|72049|6|Mentioned|p256, p259, p261, p270|||Geochronology analyses, results, and interpretation are discussed in detail.||Kurrawang Group||||
26677|Kurrawang Formation|72095|6|Mentioned|p6, p8|Neoarchean|Neoarchean|Eastern Goldfields, Yilgarn Craton.|<2657 Ma|||||
26677|Kurrawang Formation|72814|5|Briefly described|p201, Fig. 3, p202 Fig. 4|||East of Zuleika Shear, Ora Banda Domain.|||||Late basin polymictic conglomerate and cross bedded sandstone.|
26677|Kurrawang Formation|73238|5|Briefly described|p3-5, 18|||Eastern Goldfields Terrane.|c.2655 Ma (MDA).|||Unconformably overlies Kalgoorlie Sequence.||10-JAN-23
26677|Kurrawang Formation|73391|4|Described|vii, 19, 21-22, 25-26, 32, 50-51, 53|||See also p60-61, 69, 78, 86-91, 93-95, 97, 99-100, 102, 108, 110, 122, 132, 166, 172-177, 179, 182-183, 189, 192-193, 195-196, 199, 202-203, 219, 236, 242, 245, 247, 250, 253-254, 256-259, 262, 266-267, 285-286, 296, 300, 304, 310, 312, 317, 326, 332-342, 348-349, 351-352, 354, 361, 390-392, 411-412, 414, 417, 420-421, 440-441, 444-446, Appendices. Swager et al. (1990). Youngest unit of the Kalgoorlie stratigraphy, and a key stratigraphic time marker. Shown as comprising four ""major subdivisions"": Navajo Sandstone, Kurrawang Conglomerate, an un-named sandstone unit, and Kurrawang sandstone (Kurrawang Sandstone on p80, 88): a mixture of formal and informal nomenclature. Thickness ~2250m. Composite stratigraphic column; photographs. Directly identified with rocks in Africa and India. Regional stratigraphic correlation chart of previous workers.|2657 +/- 7 Ma (MDA).||Navajo sandstone; Panglo member (?).|Unconformably overlies Gibson-Honman formation (this study); Upper Black Flag Formation (previously). Correlative of the Kuttawang Formation and ?Panglo conglomerate/member.|Basal polymictic conglomerate, quartz sandstone/wacke. Contains a conglomerate unit with distinctive red jasperitic chert clasts and abundant magnetic iron-formation.|
26677|Kurrawang Formation|73453|6|Mentioned|p2|||||||||
26677|Kurrawang Formation|73596|6|Mentioned|p1161-1162|Neoarchean|Neoarchean|Kalgoorlie Terrane. Reported to have distal clast source.|2657 +/- 4 Ma (MDA).|||Overlies Merougil Formation.|Coarse clastic rocks.|
80175|Kurrparu Member|71211|4|Described|i, ix, p21, p26, p27 fig 2.3, p28-p30|Stenian|Stenian|Approximately 500m thick. Sub-divided into four facies which are described in detail. Petrography is discussed in great detail. Interpreted to be an intra-caldera ignimbrite deposit on the basis of thickness and substantial welding. See also p37-p39, p43-p54, p57-p61, p66-p68, p86-p88, p137-p138, p182, p208, p214, p265-p269. |1071 +/- 5 Ma |Kathleen Ignimbrite||Conformably overlain by the Karlaya Member. Overlies the Cleghorne Formation.|Massive, poorly-sorted, matrix supported, quartz-feldspar rhyolitic, lapilli-tuff facies.|
36835|Kuruna Member|23570|5|Briefly described|p125|Archean|Archean|Of the Maddina Basalt.  Equivalent of Kuruna Siltstone of Hickman (1983) and in this publication, of the Kuruna Siltstone Member.  Geological Province: Pilbara Craton||||||23-JUN-09
36835|Kuruna Member|23575|5|Briefly described|Map Legend|Archean|Archean|Of Maddina Formation. Underlying unit Tumbiana Formation.||||||07-NOV-08
36835|Kuruna Member|23583|5|Briefly described|Map Legend|Archean|Archean|Of Maddina Foramtion. Underlies Jeerinah Formation, including Baramine Volcanic Member. Geological Province: Hamersley Basin.||||||07-JUL-20
36835|Kuruna Member|23585|4|Described|p17|Archean|Archean|Previously Kuruna Siltstone. Of Maddina Formation. Geological Province: Hamersley Basin. Max. thickness: 70 m.||||||07-NOV-08
36835|Kuruna Member|24353|6|Mentioned|p6|Archean|Archean|Also referred to as the Kurana Siltstone. Geological Province: Pilbara Craton.||||||26-NOV-08
36835|Kuruna Member|24533|5|Briefly described|p11|Archean|Archean|Of the Maddina Formation. A distinct layer of mafic volcaniclastic sandstone, mudstone, chert and dolomite.||||||07-NOV-08
36835|Kuruna Member|24534|5|Briefly described|Map legend|Archean|Archean|Of the Maddina Formation.  Basaltic to andesitic volcaniclastic sandstone, mudstone, chert and dolomite.  Age: c.2717Ma.  Geological Province: Hamersley Basin.||||||07-NOV-08
36835|Kuruna Member|24554|6|Mentioned|p13|||||||||
36835|Kuruna Member|44229|5|Briefly described|Map legend|Archean|Archean|Of the Jeerinah Formation.  Bedded lapilli, vitric, crystal and lithic tuff, tiffaceous siltstone, and fine-grained tuffaceous sandstone.||||||07-NOV-08
36835|Kuruna Member|50131|6|Mentioned|p6 Fig. 4|||Of Fortescue Group. Geological Province: Pilbara Craton.||||||22-APR-09
36835|Kuruna Member|50146|5|Briefly described|Map Legend|Archean|Archean|Of the Maddina Formation (Fortescue Group). Geological Province: Hamersley Basin. Basaltic to andesitic volcaniclastic sandstone, mudstone, chert and dolomite.||||||07-NOV-08
36835|Kuruna Member|50189|4|Described|p23|Archean|Archean|Of the Maddina Formation. Supersedes the Kuruna Siltstone. Siliceous vitric tuff, pisolitic lapilli tuff, tuffaceous sandstone, siltstone, shale; interbedded between basalt flows of the Maddina Formation. Max. Thickness: 30m.||||||07-NOV-08
36835|Kuruna Member|50287|5|Briefly described|Map Legend|Archean|Archean|Of Maddina Formation. Geological Province: Hamersley Basin. Siltstone and tuffaceous siltstone with reworked accretionary lapelli.||||||07-NOV-08
36835|Kuruna Member|50544|4|Described|p50, p44 Fig. 8|Archean|Archean|Supersedes Kuruna Siltstone.  An important marker horizon of siliceous vitric tuff, pisolitic lapilli tuff, tuffaceous sandstone, siltstone and shale (70m thick) in top one-third of the Maddina Formation.  Geological Province: Gregory Range Inlier.||||||07-NOV-08
36835|Kuruna Member|50555|5|Briefly described|Map legend|Archean|Archean|Of the Jeerinah Formation (Fortescue Group, Mount Bruce Supergroup).  Bedded lapilli, vitric, crystal, and lithic tuff, tuffaceous siltstone and fine-grained tuffaceous sandstone.  Geological Province: Hamersley Basin.||||||07-NOV-08
36835|Kuruna Member|60373|6|Mentioned|p162|||Of Thorne and Tyler, 1996.||||||
36835|Kuruna Member|60429|4|Described|p20 Fig. 5, p21, p23|Archean|Archean|Of Maddina Formation (Fortescue Gp). Formerly the Kuruna Siltstone. Max. thickness: 30m. Distinctive horizon of siliceous vitric tuff, pisolitic lapilli tuff, tuffaceous sandstone, siltstone and shale - interbedded between basalt flows of the formation.||||||07-FEB-11
36835|Kuruna Member|63367|5|Briefly described|p234 Tb.1. |Neoarchean|Neoarchean|Trace elements and REE + Y data discussed in detail.||Of the Maddina Formation.|||Brown-weathered dolomite interbedded with siltstone and calcareous shale; stromatolites.|
36835|Kuruna Member|63372|4|Described|Map Legend|Archean|Archean|Of the Maddina Formation. Geological Province: Hamersley Basin. Mafic to volcaniclastic sandstone, mudstone, chert and dolomite. Maddina Formation over and underlies this unit.||||||07-NOV-08
36835|Kuruna Member|64654|5|Briefly described|Map Legend|Archaean|Archaean|Of Maddina Formation. Age: c. 2713Ma. Geological Province: Pilbara Craton (Hamersley Basin). Basaltic to andesitic volcaniclastic rocks (common accreationary lapilli), sandstone, siltstone, shale, and local stromatolitic limestone.||||||
36835|Kuruna Member|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Maddina Formation. Age: c. 2713Ma.  Geological Province: Hamersley Basin. Basaltic to andesitic volcaniclastic rocks (common accretionary lapilli), sandstone, siltstone, shale, and local stromatolitic limestone.||||||
36835|Kuruna Member|65724|5|Briefly described|map legend|Neoarchaean|Neoarchaean|Of Maddina Formation. Basaltic to andesitic volcaniclastic (common accretionary lapilli), sandstone, siltstone, shale, and local stromatolitic limestone. Age: c. 2713 Ma (geochronology T. S. Blake et al 2004). Geol. Prov: Hamersley Basin, Pilbara Craton.||||||
36835|Kuruna Member|65726|5|Briefly described|Map legend|Archean|Archean|Hamersley Basin, Pilbara Craton.||Of Maddina Formation.|||Bedded mafic lapilli, vitric, crystal, and lithic tuff; tuffaceous siltstone; and fine-grained tuffaceous sandstone.|
36835|Kuruna Member|65727|5|Briefly described|Map legend|Neoarchean|Neoarchean|Fortescue Basin.|c.2713 Ma (Arndt et al. 1991).|Of Maddina Formation.|||Basaltic to andesitic volcaniclastic rocks (common accretionary lapilli), sandstone, siltstone, shale and local stromatolitic limestone.|
36835|Kuruna Member|65827|3|Fully described|Tb.3 p12, p33 Fig.6, p39, p40|Neoarchean|Neoarchean|Thorne and Trendall (2001). Of Maddina Formation (Fortescue Group). Formerly Kuruna Siltstone (MacLeod and de la Hunty, 1966). c.2713 Ma. Shown as equivalent to part of Mount Jope Supersequence(2). Volcaniclastic sandstone and siltstone interbedded with felsic lapilli tuffs; intruded by thick dolerite sills.||||||
36835|Kuruna Member|65828|5|Briefly described|Map legend|Archean|Archean|||Unit in Maddina Formation.|||Siltstone and tuffaceous siltstone with reworked accretionary lapilli.|
36835|Kuruna Member|65829|3|Fully described|p10, pp21-22.|Neoarchean|Neoarchean|Formerly Kuruna Siltstone (MacLeod and de la Hunty 1966). A prominent marker horizon in upper Maddina Formation. Intruded by thick dolerite sills and dykes.|c.2713 Ma.|Unit in Maddina Formation.||Overlies Tumbiana Formation.|Fine- to medium-grained, volcaniclastic, basaltic and andesitic rocks including accretionary lapilli, siltstone, shale, fine-grained sandstone and partly silicified stromatolitic carbonate.|
36835|Kuruna Member|66108|5|Briefly described|Map legend|Neoarchean|Neoarchean|Unit in Maddina Formation, Fortescue Group. c. 2713 Ma. Basaltic to andesitic volcaniclastic rocks (common accretionary lapilli), sandstone, siltstone, shale, and local stromatolitic limestone.||||||15-APR-13
36835|Kuruna Member|66685|5|Briefly described|p217 Fig.2|Archean|Archean|||Maddina Formation|||Sandstone with stromatolites.|
36835|Kuruna Member|67201|5|Briefly described|p29 Fig.15|||Northern Fortescue Basin, Northeast Pilbara Sub-basin.||Maddina Formation||||
36835|Kuruna Member|68056|5|Briefly described|p171, 176, 188, 190|Archean|Archean|Pilbara Craton. Organic and inorganic C isotope analyses tabulated.||Maddina Formation.|||Conglomerate, calcareous and tuffaceous sandstones, and black siliceous mudstone.|
36835|Kuruna Member|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Maddina Formation|||Basaltic to andesitic volcaniclastic rocks (common accretionary lapilli), sandstone, siltstone, shale, and local stromatolitic limestone|
36835|Kuruna Member|69299|6|Mentioned|p19|||Previously Kuruna Siltstone (Hickman 1983). This unit is not shown on 1:100 000 COOYA POOYA map [probably doesn't crop out here].||Of Maddina Formation.|||Sedimentary.|
36835|Kuruna Member|69301|6|Mentioned|p18 Fig.7|||Pilbara Craton. Fortescue Basin. Northeast Pilbara Sub-basin, Sequence 3.||||||
36835|Kuruna Member|69590|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Of Northeast Pilbara Sub-basin, Fortescue Basin. Events: Pilbara Craton breakup. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|2718-2713 Ma inferred)|Unit of Maddina Formation.|||Basaltic to andesitic volcaniclastic rocks (common accretionary lapilli), sandstone, siltstone, shale, and local stromatolitic limestone|
36835|Kuruna Member|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||volcaniclastic rock, mudstone, chert, crystalline dolostone/dolomite|
36835|Kuruna Member|71808|6|Mentioned|p8|||Pilbara Craton.||Maddina Formation|||Tuffaceous rocks.|
31778|Kutakuta Tonalite|50436|5|Briefly described|p1.3, 3.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of the Krackatinny Supersuite.||||||
25141|Kwinana Group|12759|6|Mentioned|p33 Fig.16, p43-51|Quaternary|Quaternary|With Ascot Formation, referred to in WA as 'superficial formations' (Allen, 1976).|||Includes Yoganup Formation, Tamala Limestone, Guildford Clay; Gnangara, Bassendean, Becher and Safety Bay Sands.|||
25141|Kwinana Group|24410|5|Briefly described|p39|Quaternary|Quaternary|Geological Province: Perth Basin.||||||24-NOV-09
25141|Kwinana Group|35970|6|Mentioned|p77|||See also Table 12.||||||
25141|Kwinana Group|36293|2|Defined|p208|early Pleistocene|late Tertiary|Holocene to early Pleistocene or late Tertiary.||||||
25141|Kwinana Group|37308|5|Briefly described|Table 4|||Hydrogeology p25.||||||07-AUG-07
25141|Kwinana Group|37309|5|Briefly described|p16|||Groundwater p17.||||||07-AUG-07
25141|Kwinana Group|38479|4|Described|p16|||||||||
25141|Kwinana Group|40367|6|Mentioned|p72|Quaternary|Quaternary|Includes Australind Formation, Tamala Limestone, Eaton Sand, Leschenault Formation and Safety Bay Sand.||||||07-AUG-07
25141|Kwinana Group|40395|6|Mentioned|p332|||||||||
25141|Kwinana Group|41831|5|Briefly described|p556|||||||||
25141|Kwinana Group|44144|5|Briefly described|p501 Tb.4-21, p518 fig 4-162, p520|Quaternary|Quaternary|Playford et al. (1976).|||Ridge Hill Sandstone, Bassendean Sand, Safety Bay Sand, Cooloongup Sand, Herschell Limestone, Tamala Limestone, Peppermint Grove Limestone, Rottnest Limestone.|Overlies Wadjemup Formation.||
25141|Kwinana Group|61155|5|Briefly described|p15|Pleistocene|Late Pliocene|Age: <2Ma. Geological Province: Perth Basin.||||||
25141|Kwinana Group|64580|6|Mentioned|map legend|||||||||
25141|Kwinana Group|70128|5|Briefly described|p449|Holocene|Neogene|Perth Basin.||||Unconformably overlies Kings Park Formation.||
25141|Kwinana Group|70826|6|Mentioned|p7 tbl 4|Quaternary|Quaternary|Perth Basin.||||||
25141|Kwinana Group|72034|6|Mentioned|500k_interpgeop16_lut|Pleistocene|Pleistocene|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Tamala Limestone.|||
73929|Kyarra Basalt|62108|5|Briefly described|p1409 Tb. 9|||Of the Kalgoorlie Group. Geological Province: Yilgarn Craton (Boulder-Lefroy Shear Zone).||||||07-FEB-11
73929|Kyarra Basalt|73391|6|Mentioned|Appendices.|||Langsford (1989). Regional stratigraphic correlation chart of other workers.|||||Lower high-Mg basalt, massive unpillowed; upper massive basalt, thin interflow sedimentary rocks, abundant pillow lava and flow-top breccia.|
34040|Kylena Formation|22475|5|Briefly described|Fig.3|Archean|Archean|Part of Lower Fortescue Group.||||||07-NOV-08
34040|Kylena Formation|23416|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. In the Hamersley Basin.||||||07-NOV-08
34040|Kylena Formation|23484|6|Mentioned|p26|||||||||
34040|Kylena Formation|23570|3|Fully described|p83, p151, p235 App. 1|Archean|Archean|Of Fortescue Group. Name replaces Kylena Basalt, Kylena Basalt Member and Kylena Volcanics. However all terms used throughout the text. Correlated with Boongal Fm. Geol.prov: Hamersley Basin. Overlain by Tumbiana Fm; underlain by Hardey Fm.||||||07-NOV-08
34040|Kylena Formation|23575|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Overlain by Tumbiana Formation. Underlain by Hardey Formation.||||||07-NOV-08
34040|Kylena Formation|23583|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Underlain by Hardey Formation. Geological Province Hamersley Basin.||||||07-NOV-08
34040|Kylena Formation|23585|3|Fully described|p16|Archean|Archean|Previously Kylena Basalt. Of Fortescue Group. Overlain by Tumbiana Formation. Underlain by Hardey Formation. Geol. Prov: Hamersley Basin. Max. thickness: 1300 m.||||||07-NOV-08
34040|Kylena Formation|23598|4|Described|p13|||Previously Kylena Basalt. Of Fortescue Group. Overlain by Tumbiana Formation. Underlain by Hardey Formation. Geological Province: Pilbara Craton.||||||16-JAN-07
34040|Kylena Formation|23755|4|Described|p57|Archean|Archean|See also page 17 table 1. Of Fortescue Group.||||||07-NOV-08
34040|Kylena Formation|23783|5|Briefly described|p115 Fig. 64|Archean|Archean|Of Fortescue Group.||||||07-NOV-08
34040|Kylena Formation|23784|5|Briefly described|p4 Tb. 1|Archean|Archean|||||||07-NOV-08
34040|Kylena Formation|23789|6|Mentioned|p32|||||||||
34040|Kylena Formation|23813|5|Briefly described|p112|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
34040|Kylena Formation|24025|5|Briefly described|p14|Archean|Archean|Of Fortescue Group.  Geological Province: Hamersley Basin.||||||07-NOV-08
34040|Kylena Formation|24110|5|Briefly described|Plate 1|Archean|Archean|Of the Fortescue Group. Geological Province: Hamersley Basin.||||||07-NOV-08
34040|Kylena Formation|24352|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group.   Age: ~2760Ma.  Massive or amygdaloidal basalt, basaltic andesite and dacite; local high-Mg basalt and rhyolite. Geological Province: Hamersley Basin||||||07-NOV-08
34040|Kylena Formation|24353|4|Described|p1, p9 Fig.5, p11 Tb.2|Archean|Archean|Locally intruded by the Cooya Pooya Dolerite. Age: <2750Ma. Of the Fortescue Group. Max Thickness: 520m. Geological Province: Pilbara Craton||||||07-NOV-08
34040|Kylena Formation|24531|5|Briefly described|p36|Archean|Archean|Name used interchangeably with Kylena Basalt.  Age: c.2747Ma.||||||07-NOV-08
34040|Kylena Formation|24533|5|Briefly described|p6, 9|Archean|Archean|Of Fortescue Group. Overlies Hardey Formation; overlain conformably by Tumbiana Formation. Typically comprises flows of massive to amygdaloidal basalt and basaltic andesite. Geological Province: Hamersley Basin.||||||07-NOV-08
34040|Kylena Formation|24534|5|Briefly described|Map legend|Archean|Archean|Of Fortescue Group.  Massive and amygdaloidal basalt, baslatic andesite and dacite.  Geological Province: Hamersley Basin.||||||07-NOV-08
34040|Kylena Formation|24541|3|Fully described|p11 Tb.2, p50-51|Paleoproterozoic|Neoarchean|Of the Fortescue Group. Age: c. 2750-2730 Ma. Overlain by Tumbiana Formation. Maximum Thickness: 500m. Unconformably overlies the Dampier Granitoid Complex and conformably overlies the Hardey Formation.||||||07-NOV-08
34040|Kylena Formation|24543|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group (Mount Bruce Supergroup).  Age: >2719Ma.  Basalt, basaltic andesite, and dacite.||||||07-NOV-08
34040|Kylena Formation|24554|4|Described|p5, p12|||Formerly Kylena Basalt. Conformably or disconformably overlies the Hardey Formation on SATRIST. Of the Fortescue Group. Geological Province: Hamersley Basin, Pilbara Craton.||||||
34040|Kylena Formation|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Of the Fortescue Group. Thick flows of basalt. Age: >/=2756Ma.||||||07-FEB-11
34040|Kylena Formation|44229|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group. Massive, vesicluar and amygdaloidal basalt and andesite.||||||18-JUN-14
34040|Kylena Formation|50146|5|Briefly described|Map Legend|Archean|Archean|Of the Fortescue Group. Geological Province: Hamersley Basin. Massive and amygdaloidal basalt, basaltic andesite, and dacite; local high-Mg basalt and rhyolite.||||||07-NOV-08
34040|Kylena Formation|50189|4|Described|p22|Archean|Archean|Of the Fortescue Group. Supersedes the Kylena Basalt. Consists of mainly dark-grey to grey-green, massive, amygdaloidal basalt and basaltic andesite. Max. thickness: 1300m.||||||07-NOV-08
34040|Kylena Formation|50287|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group (Mount Bruce Supergroup). Geological Province: Hamersley Basin.||||||07-NOV-08
34040|Kylena Formation|50300|5|Briefly described|Map Legend|Archean|Archean|Of the Fortescue Group.  Geological Province: Hamersley Basin.  Interbedded with Cooya Pooya Dolerite.||||||07-NOV-08
34040|Kylena Formation|50370|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group (Mount Bruce Supergroup). Geological Province: Hamersley Basin, Pilbara Craton.||||||07-NOV-08
34040|Kylena Formation|50381|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group (Mount Bruce Supergroup). Geological Province: Hamersley Basin, Pilbara Craton.||||||07-NOV-08
34040|Kylena Formation|50382|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Geological Province: Hamersley Basin, Pilbara Craton.||||||07-NOV-08
34040|Kylena Formation|50427|6|Mentioned|p188 Fig.9|Archean|Archean|Of Fortescue Group.||||||07-NOV-08
34040|Kylena Formation|50544|3|Fully described|p47-48, p15 Tb. 1|Archean|Archean|Supersedes Kylena Basalt.  Of Fortescue Group.  Volcaniclastic lacustrine deposits.  Disconformable over Bamboo Creek Mbr. in Oakover Syncline area; unconformabe over Koongaling Volcanic Mbr.in Gregory Range Inlier.  Age: ~2741Ma.  Max. thick: 1300m.||||||07-NOV-08
34040|Kylena Formation|50555|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group (Mount Bruce Supergroup).  Massive, vesicular and amygdaloidal basalt and andesite.  Age: c.2741Ma.  Geological Province: Hamersley Basin.||||||07-NOV-08
34040|Kylena Formation|60373|4|Described|p145 Tb. 1, p150 Tb. 2, p164|Archean|Archean|Of Fortescue Group. Overlian by Tumbiana Formation, underlain by Hardey Formation. Age: 2760+/-10Ma (SHRIMP, Arndt et al., 1991). It is likely that the Kylena Basalt and this unit are the same.||||||
34040|Kylena Formation|60429|4|Described|p20 Fig. 5, p21 p22|Archean|Archean|Of Kojan and Hickman (1998). Of the Fortescue Group. Supersedes Kylena Basalt. Overlies Hardey Formation; underlies Kylena Formation. Max. thickness: 1300m. Mainly massive, amygdaloidal basalt and basaltic andesite. Detailed lithology included.||||||07-FEB-11
34040|Kylena Formation|60635|6|Mentioned|p51 Fig. 2.2A|||||||||
34040|Kylena Formation|61259|5|Briefly described|p404 Fig. 1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
34040|Kylena Formation|61265|4|Described|p43, p46-47 Fig.2|||Supersedes the Kylena Basalt. Of the Fortescue Group. Locally overlain by the Tumbiana Formation. Trachyandesite, dacite, rhyolite and basalt. Max. thickness: ~520m. Geological: Province: Pilbara Craton.||||||
34040|Kylena Formation|61266|4|Described|p58 Tb.1, p59|Archean|Archean|Of the Fortescue Group. Age: >2715 Ma (Arndt et al., 1991). Thick flows of basalt. Geological Province: Pilbara Craton.||||||07-NOV-08
34040|Kylena Formation|61268|5|Briefly described|p79, p81 Tb.1|||Of the Fortescue Group. Overlies the Dampier Granitoid Complex with an angular unconformity. Lower part composed of basalt and basaltic andesite, upper 150m ranges from andesite to dacite. See also p80 Fig.2, p83 Fig.4.||||||
34040|Kylena Formation|62576|5|Briefly described|p618 Fig. 1, p619|Archean|Archean|Of the Fortescue Group. Age: ca 2740Ma. Geological province: Pilbara Craton. See also p620 Fig. 3.||||||07-NOV-08
34040|Kylena Formation|63367|5|Briefly described|p230, p231 Fig.1, p233 Fig.3, p236 |Neoarchean|Neoarchean|Marble Bar sub-basin. Exposures show pillows at the base of the Formation. Trace elements and REE + Y data discussed in detail.|2.74 Ga|Unit in Fortescue Group.|Includes the Mopoke Member.||Flood basalt sequence; subaqueous flows overlain by subaerial flows.|
34040|Kylena Formation|63372|4|Described|Map Legend|Archean|Archean|Of the Fortescue Group. Geological Province: Hamersley Basin. Age: 2741Ma. Underlies Tumbiana Formation. Massive or amygdaloidal basalt, basaltic andesite, and dacite; local komatiitic basalt and rhyolite.||||||07-NOV-08
34040|Kylena Formation|63417|5|Briefly described|Map legend|Archean|Archean|Of Fortescue Group (Mount Bruce Supergroup). Age: 2749-2735Ma. Geological Province: Fortescue Basin. Massive; amygdaloidal, or vesicular basalt and basaltic andesite; local komatiitic basalt, dacite and rhyolite.||||||07-NOV-08
34040|Kylena Formation|63420|5|Briefly described|Map legend|Archean|Archean|Of Fortescue Group (Mount Bruce Supergroup).Overlies Mount Roe Basalt. Age: c.2741Ma. Geol.Prov: Marble Bar Sub-basin/Hamersley Basin. Massive and vesicular tholeiitic basalt to basaltic andesite; thick flows....||||||07-NOV-08
34040|Kylena Formation|63866|5|Briefly described|p144|||Eastern Pilbara Granite-Greenstone Terrane.||Fortescue Group||||
34040|Kylena Formation|64326|5|Briefly described|p71 Fig. 1, p73|Archean|Archean|Of the Fortescue Gp (Mount Bruce Supergp). Stratigraphic detail describes Kylena Fm as it presents in the Pear Creek Centrocline (northern Hamersley Basin) - where the Fortescue Group succession is different from elsewhere. Unconformable over Hardey Fm||||||07-FEB-11
34040|Kylena Formation|64580|4|Described|map legend||Neoarchean|Of Fortescue Group, massive, amygdaloidal, and vesicular basalt and basaltic andesite; local komatiitic basalt, dacite and rhyolite.||||||26-NOV-08
34040|Kylena Formation|64621|5|Briefly described|Map legend|Archean|Archean|Of Fortescue Group. Age: 2749-2735Ma. Massive + vesicular tholeiitic basaltic andesite, thick flows; pillow basalt; basaltic pillow breccia (mostly angular fragments, local full pillows) in matrix of welded basaltic glass shards; dolerite, etc.||||||07-NOV-08
34040|Kylena Formation|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Age: 2764-2756Ma. Geological Province: Pilbara Craton. Massive, vescular, and amygdaloidal basalt; some pillow lava and columnar jointing; minor basaltic agglomerate.||||||07-FEB-11
34040|Kylena Formation|64654|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Age: 2749Ma - 2735Ma. Geological Province: Pilbara Craton (Hamersley Basin). Massive to vesicular basalt, quartz sandstone, coarse pillow breccia with fine-grained hyaloclastites; sandy matrix.||||||17-NOV-08
34040|Kylena Formation|64656|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Age: 2749-2735Ma. Geological Province: Hamersley Basin. Massive and amygdaloidal basaltic andesite; minor basalt and andesite; minor basaltic fragmental rock.||||||
34040|Kylena Formation|64936|5|Briefly described|map legend|Archean|Archean|Of Fortescue Group, Mount Bruce Supergroup. Under Pear Creek Formation; over Hardey Formation. Massive and vesicular basalt. Age: c. 2741 Ma (geochronology: TS Blake 2001). Geol. Prov: Hamersley Basin, Pilbara Craton.||||||
34040|Kylena Formation|65008|4|Described|p7, p8 Fig.5, p21, p23, p24, p41|Neoarchean|Neoarchean|Hamersley Basin. Geochronology by: T.S. Blake, 2001, Precambrian Research, v. 107, p139-177. Includes an unnamed subunit. ~500m thick.|ca. 2741 Ma|Of the Fortescue Group||Conformably underlain by the Hardey Formation. Overlain by the Tumbiana Formation.|Undivided: massive, vesicular, and amygdaloidal basalt; some pillow lava and columnar jointing; minor basaltic agglomerate. Separately mapped are: massive and amygdaloidal basaltic andesite; minor basalt and andesite; rare basaltic fragmental rock.|
34040|Kylena Formation|65724|5|Briefly described|map legend|Neoarchaean|Neoarchaean|Of Fortescue Group. Includes Mopoke Member. Under Tumbiana Fm; over Hardey Fm, Cleland Supersuite and Elsie Creek Tonalite. Basalt and basaltic andesite. Age: 2749-2735 Ma (geochron 3 sources). Geol. Prov: Hamersley Basin, Pilbara Craton.||||||
34040|Kylena Formation|65726|5|Briefly described|Map legend|Archean|Archean|Hamersley Basin, Pilbara Craton.|c.2741 Ma.|Of Fortescue Group. |Includes Mopoke Member.|Is overlain by Mingah Member of the Tumbiana Formation.|Massive, vesicular, and amygdaloidal basalt and andesite; local pillow basalt and komatiitic basalt.|
34040|Kylena Formation|65727|5|Briefly described|Map legend|Neoarchean|Neoarchean|Fortescue Basin.|2749 - 2735 Ma (Arndt et al. 1991).|Of Fortescue Group. |Includes Mopoke Member.|Is overlain by Mingah Member of the Tumbiana Formation.|Massive, vesicular, and amygdaloidal basalt and andesite; local komatiitic basalt, dacite and rhyolite.|
34040|Kylena Formation|65825|4|Described|p4, p7 Fig.4,  pp21-22. |Archean|Archean|Mafic rocks are petrographically similar to the basalts of the Mount Roe basalt. The more differentiated volcanic rocks are towards the top of the succession: the uppermost part has Th content similar to Bamboo Creek Member, and K content comparable to parts of Yilgalong Granitic Complex.|Between 2741 +/- 3 Ma and c.2724 - 2715 Ma.|Unit in Fortescue Group.||Unconformably overlies Yilgalong Granitic Complex, Mosquito Creek Formation, Golden Eagle Orthogneiss and Hardey Formation. Is overlain conformably by Tumbiana Formation.|A lower succession of basalt, local mafic tuff, probable komatiitic basalt, thin unit of stromatolitic limestone, interbedded calcareous shale and siltstone; and an upper succession of tholeiitic basalt, basaltic andesite and andesite.|
34040|Kylena Formation|65827|3|Fully described|p12 Tb.3, p32, p33 Fig.6, p36-37|Neoarchean|Neoarchean|Kojan and Hickman (1998). Of Fortescue Group; formerly Kylena Basalt. Includes Mopoke Member. 2749-2735 Ma. Unconformably overlies Hardey Fm, Mount Roe Basalt; conformably or disconformably underlies Tumbiana Fm; shown as equivalent to part of Nullagine Supersequence;  intruded by Bridget Suite. Subaerial basaltic fissure eruptions. Lower succession of komatiitic basalt; upper succession of basalt and basaltic andesite; separated by Mopoke Member.||||||
34040|Kylena Formation|65828|5|Briefly described|Map legend|Archean|Archean|||Unit in Fortescue Group.||Is overlain by Tumbiana Formation.|Massive and amygdaloidal basaltic andesite; minor basalt and andesite; rare basaltic fragmental rock.|
34040|Kylena Formation|65829|3|Fully described|p4, p7 Fig.3, pp17-18. |Neoarchean|Neoarchean|Formerly Kylena Basalt (Nullagine 1:250 00 sheet, Hickman 1978). Part of Nullagine Supersequence (Blake et al. 2004). Mostly subaerial and local subaqueous basaltic and komatiitic fissure eruptions. Well exposed in a broad area of the map. Thickness to 1800 m. The lower basaltic succession has a distinctive low K, Th radiometric pseudocolour in contrast with the upper succession with high K and Th.|c.2749 - c.2735 Ma (Nelson; Bordokos).|Unit in Fortescue Group.|Includes Mopoke Member.|Overlies unconformably the Hardey Formation.|Predominantly tholeiitic basalt with lesser komatiitic basalt, basaltic andesite, and dacite; lower portion contains a distinctive carbonate marker horizon: the Mopoke Member.|
34040|Kylena Formation|66108|5|Briefly described|Map legend|Neoarchean|Neoarchean|Unit in Fortescue Group. 2749-2735 Ma. Massive, amygdaloidal, and vesicular basalt and basaltic andesite; local komatiitic basalt, dacite and rhyolite.||||||
34040|Kylena Formation|66217|4|Described|p5, p6 Table 1, pp45-48, pp52-55.|Neoarchean|Neoarchean|Fortescue Basin, Pilbara Craton. Also called Kylena Basalt on p.37. Thickness to 1300 m.|2741 +/- 3 Ma (Blake et al. 2004).|Unit in Fortescue Group.||Unconformably overlies Hardey Formation and Mount Roe Basalt. Is unconformably overlain by Pear Creek Formation.|Subaerial basaltic andesite to basaltic flows; includes locally significant basaltic pillow breccia deposits, pillowed successions, interflow clastic sedimentary rocks, minor stromatolitic carbonate rocks and volcaniclastic sedimentary rocks.|
34040|Kylena Formation|66685|5|Briefly described|p217 Fig.2; p218|Archean|Archean||2741 +/- 3 Ma (zircon U-Pb, Blake et al., 2004).|Fortescue Group||Overlies Hardey Formation. Underlies (conformably and unconformably) the Mingah Member (Tumbiana Formation).|Includes basalt.|
34040|Kylena Formation|67130|5|Briefly described|p3 fig 2, p48|Neoarchean|Neoarchean||2741 Ma  +/- 3 Ma|Fortescue Group||Overlies Hardey Formation, Overlain by Tumbiana Formation|Basalt.|
34040|Kylena Formation|67183|6|Mentioned|p645 Tb.1|Archean|Archean|Present in the Southern Pilbara and Oakover Basin. Formerly Kylena Basalt (see also p643, p651).||Fortescue Group||||
34040|Kylena Formation|67201|4|Described|p28-30, p50-51|||Northern Fortescue Basin, Northeast and Northwest Pilbara Sub-basins. Thickness: ~ 250 m (individual flows are 10-25 m thick). Composition of Cooya Pooya Dolerite is very similar to lower Kylena Formation.||Fortescue Group|Gidley Granophyre|Unconformably overlies Hardey Formation. Is overlain by Tumbiana Formation apparently conformably, locally unconformably. Intruded by Cooya Pooya Dolerite. Equivalent to Boongal Formation.|Ultramafic-mafic-felsic volcanic cycles including komatiitic basalt, basalt, andesite, dacite and local rhyolite.|24-NOV-16
34040|Kylena Formation|67229|5|Briefly described|p4, p13-14|||||||Is overlain conformably by Tumbiana Formation.|Widespread subaerial and subaqueous basalt flows and volcaniclastic rocks.|
34040|Kylena Formation|67269|5|Briefly described|p5|Paleoarchean|Paleoarchean|||Fortescue Group.|||Basalt and dolerite dykes.|
34040|Kylena Formation|68035|5|Briefly described|p293, p292 Fig 6|Neoarchean|Neoarchean|Fortescue Basin. Widespread stromatolites in lacustrine carbonate units. Also microbial structures described.|2741 +/-3 Ma|Fortescue Group||Overlies Hardey Formation, overlain by Tumbiana  Formation.|Basalt.|
34040|Kylena Formation|68056|6|Mentioned|p170-171|Archean|Archean|Pilbara Craton.||Fortescue Group.||||
34040|Kylena Formation|68101|4|Described|p1-4, p6-8|Neoarchean|Neoarchean|0-1300m thick. The two lava flows, separated by the Mopoke Member, are compositionally distinct. Three age determinations range from 2749 +/- 5 Ma (Nelson et al., 2006) to 2735 +/- 6 Ma (Bodorkos et al., 2006).|c.2740 Ma.|Fortescue Group|Includes Mopoke Member|Disconformably overlain by Tumbiana Formation; unconformably overlies Hardey Formation. Equivalent to Boongal Formation.|Subaerial basaltic lava flows separated by carbonate, volcaniclastic and siliciclastic sedimentary rocks. Lava flows are typically massive with highly vesicular, amygdaloidal and scoriaceous flow tops.|
34040|Kylena Formation|68280|5|Briefly described|p5|Neoarchean|Neoarchean||2741 +/- 3 Ma|Fortescue Group||Overlain by Tumbiana Formation, overlies Hardey Formation|Basalt.|
34040|Kylena Formation|68281|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.|2749-2735 Ma (Blake, 2001).|Of the Fortescue Group.||Dolerite sills intrude the Hardey Formation.|Massive and vesicular tholeiitic basalt to basaltic andesite (thick flows); basaltic fragmental rock; dolerite (commonly as sills with baked contacts, and as dykes; commonly amygdaloidal and with local columnar jointing).|02-DEC-14
34040|Kylena Formation|68283|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Marble Bar Sub-basin, Fortescue Basin.|c. 2741 Ma (Blake, 2001).|Of the Fortescue Group.|||Massive and vesicular tholeiitic basalt to basaltic andesite (thick flows); brecciated pillow basalt with fine-grained hyaloclastitic to sandy matrix.|
34040|Kylena Formation|69012|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.|2749-2735 Ma (Blake et al., 2004)|Of the Fortescue Group.|||Massive, amygdaloidal, and vesicular basalt and basaltic andesite; local komatiitic basalt, dacite, and rhyolite.|29-APR-14
34040|Kylena Formation|69015|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin. Mapped as 3 unnamed sub-units.|2749-2735 Ma (Arndt et al., 1991)|Of the Fortescue Group.|||Massive and vesicular tholeiitic basalt to basaltic andesite, thick flows; basaltic fragmental rock; dolerite sills and dykes, commonly amygdaloidal, local columnar jointing.|05-MAY-14
34040|Kylena Formation|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|Age derived from sample of dacite (178086.1.pdf) which is part of a distinctive felsic unit underlying the mopoke member. Intruded by unnamed quartz monzonites.|2749+/- 5 Ma (SHRIMP)|Fortescue Group|Includes Mopoke Member||Massive, amygdaloidal, vesicular and pillow basalts and basaltic andesite; dacite, and rhyolite. Quartz and pebbly sandstones, rhyolite, rhyolitic and basaltic volcaniclastic rocks, rhyolitic and basaltic breccias, dolerite dykes and sills.|
34040|Kylena Formation|69185|4|Described|GEOL_LUT_CSV files||Neoarchean|Geological Province: Pilbara Craton. Of Northwest, Northeast, and South Pilbara Sub-basins, Hamersley Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.||Unit of Fortescue Group.|||Undivided; massive, amygdaloidal, and vesicular basalt and basaltic andesite; local komatiitic basalt, dacite and rhyolite|
34040|Kylena Formation|69299|3|Fully described|p1,p4-7,p9,p14-21, map, Fig.4,Tb.1,Tb.2|Archean|Archean|Formerly Kylena Basalt. A dominantly basaltic to andesitic magmatic event at 2750-2740 Ma resulted in eruption of Kylena Formation and comagmatic intrusion of Cooya Pooya Dolerite. On COOYA POOYA, mapping indicates that both lower and upper sills of Cooya Pooya Dolerite are comagmatic with Kylena Formation. Thickness on COOYA POOYA: 0-200 m. Geol. Prov: Hamersley Basin, Pilbara Craton.|c. 2750-2740 Ma|Of Fortescue Group.||Comagmatic with Cooya Pooya Dolerite (lower Kylena Formation is intruded by Cooya Pooya Dolerite sills); is locally overlain (angular unconformity) by Tumbiana Formation.|Massive or amygdaloidal basalt, basaltic andesite, andesite, dacite, and rhyolite; local high-Mg basalt.|01-JUL-14
34040|Kylena Formation|69301|4|Described|p16-18, p22|||Pilbara Craton. Fortescue Basin. Northeast Pilbara Sub-basin, Northwest Pilbara Sub-basin, Sequence 3. Thickness: several hundres of metres.|ca. 2.74 Ga|Fortescue Group||Is overlain by Tumbiana Formation.|Dominantly volcanic. Composed of ultramafic-mafic-felsic volcanic cycles.|
34040|Kylena Formation|69411|5|Briefly described|p282,286|Neoarchean|Neoarchean|Geological province: Pilbara Craton.|2741+\-3 Ma (U-Pb, Blake et al., 2004)|Unit of Fortescue Group.|Includes Mopoke Member.|Overlain conformably by Tumbiana Formation.|Subaerial and subaqueous basaltic lava and volcaniclastic rocks.|05-JUL-19
34040|Kylena Formation|69563|5|Briefly described|p699||||c.2749-2735 Ma.|Unit in Fortescue Group.||||
34040|Kylena Formation|69569|6|Mentioned|p285 Fig.1|||East Pilbara Terrane.||Fortescue Group.||||
34040|Kylena Formation|69590|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Of Northeast Pilbara Sub-basin, Fortescue Basin. Events: Pilbara Craton breakup. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeol_lut.csv.|2749-2735 Ma (isotopic, inferred)|Unit of Fortescue Group.|Includes Mopoke Member.|Intruded by Bridget Suite.|Basalt; massive, amygdaloidal, komatiitic, tholeiitic, pillow breccia; andesite and basaltic andesite; rhyolite, rhyolitic volcanic breccia and volcaniclastics; conglomerate, sandstone, siltstone, shale, lapilli, felsic tuffs.|
34040|Kylena Formation|69792|5|Briefly described|p1095-8, p1100, p1101 Fig.7, p1103-07|Neoarchean|Neoarchean|Formerly Kylena Basalt.|c. 2740 Ma|Unit in Fortescue Group.|Includes Mopoke Member.|Disconformably underlies Hardey Formation. Is disconformably overlain by Tumbiana Formation.|Subaerial lava flows and thin unit of carbonate, volcaniclastic and siliciclastic sedimentary rocks.|06-APR-22
34040|Kylena Formation|70795|6|Mentioned|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean||2749-2730 Ma|||||
34040|Kylena Formation|71042|5|Briefly described|p66, p71-p72|Archean|Archean|Oakover Basin, Southern Pilbara.||Fortescue Group||||
34040|Kylena Formation|71169|5|Briefly described|p64|Neoarchean|Neoarchean|Pilbara Craton. Age is interpreted as the age of a tuffaceous compoenent. Detrital ages between c. 3391 and 2781 Ma are also given in Bodorkos et al., 2006.|2735 +/- 6 Ma (Bodorkos et al., 2006)|Fortescue Group|||Volcaniclastic sandstone.|
34040|Kylena Formation|71267|5|Briefly described|1m_geologyp12_lithology_lut.csv||||||||basalt, andesite, rhyolite, dacite|22-JUN-20
34040|Kylena Formation|71803|4|Described|p365-p368, p371, p375, p380|Neoarchean|Neoarchean|Pilbara Craton. Geochemsitry discussed. An age of 2760 +/- 10 Ma is derived for the base of this unit from Arndt et al, 1991.|2740 Ma|Fortescue Group||Laterally equivalent to the Boongal Formation.|Abundant mafic lavas including both subaerial, subaqueous flows with mafic volcaniclastic rocks, lesser andesite and rhyolite and minor carbonates.|
34040|Kylena Formation|71808|5|Briefly described|p7|||Pilbara Craton. Basalt was deposited in both subaerial and submarine environments.||Fortescue Group|||Basalt and andesite.|
34040|Kylena Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Marble Bar Sub-basin; Northeast Pilbara Sub-basin; Northwest Pilbara Sub-basin, Fortescue Basin.|Max age 2749+/- 5 Ma, min 2735+/-5 Ma.|Fortescue Group, sequence 3|Includes Cooya Pooya Dolerite.||Massive, amygdaloidal, and vesicular basalt and basaltic andesite; local komatiitic basalt, dacite, and rhyolite.|
34040|Kylena Formation|72489|6|Mentioned|p12|Archean|Archean|||||||
34040|Kylena Formation|72712|6|Mentioned|p10 Fig.6.|Neoarchean|Neoarchean|Shown only on p10 Fig.6 diagrammatically as the northern equivalent to the Boongal Formation. See also Kylena Basalt p8.|c. 2745 Ma to c. 2715 Ma.|||Underlies Tumbiana Formation and is equivalent to Boongal Formation.|Shown as basalt.|
34040|Kylena Formation|73538|6|Mentioned|p4|Neoarchean|Neoarchean|Written as Kylena Formation / Boongali Formation. An age of 2760 +/- 10 Ma was reported by Mole et al. (2018) for these units.|2760 +/- 10 Ma|Fortescue Group||Underlain by Hardey Formation. Overlain by Pyradie Formation / Tumbiana Formation.|Mafic volcanics.|
80947|Kynea Migmatite|73410|6|Mentioned|p2|||Youanmi Terrane.|2960 +/- 10 Ma (Lu et al., 2017).|||||
25983|Labouchere Formation|7161|6|Mentioned|p96 Fig.6|||Less than 3000m thick (from p96 Fig.6).||||Overlain by the Wilthorpe Formation.||
25983|Labouchere Formation|12099|5|Briefly described|p678 Fig.4, p682-3|Statherian|Orosirian|Interpreted by Martin (1994) to be an upward-coarsening, deep-water turbidite complex derived from Yilgarn Craton material and underlying rocks of the Bryah Basin. Placed in Glengarry Group by Gee (1987).||Unit in Padbury Group.||Overlies Bryah Group. Is overlain by Wilthorpe Formation.||04-MAR-13
25983|Labouchere Formation|22493|5|Briefly described|p96 Fig.6|||||||||
25983|Labouchere Formation|22694|5|Briefly described|p7|||||||||
25983|Labouchere Formation|22940|3|Fully described|p16, Fig.6 p14|Paleoproterozoic|Paleoproterozoic|Age of unit 2.0-1.9 Ga (Windh, 1992). See also Table 2 p12, p10. Of Padbury Group.||||||07-NOV-08
25983|Labouchere Formation|23592|5|Briefly described|p12|||Of Padbury Group. Geological Province: Padbury Basin.||||||
25983|Labouchere Formation|23744|4|Described|p13|Paleoproterozoic|Paleoproterozoic|Of Padbury Group. Geological Province: Padbury Basin. Max thickness: 4000 m.||||||07-NOV-08
25983|Labouchere Formation|23747|4|Described|p15|Paleoproterozoic|Paleoproterozoic|Of Padbury Group. Geological Province: Padbury Basin. Max. thickness: 5000 m.||||||07-NOV-08
25983|Labouchere Formation|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Padbury Group. Geological Province: Padbury Basin||||||
25983|Labouchere Formation|23749|5|Briefly described|p3 table 1|||Of Padbury Group. Geological Province: Padbury Basin.||||||28-NOV-06
25983|Labouchere Formation|23890|5|Briefly described|p21 Fig.11|||Of Padbury Group. Geological Province: Padbury Basin.||||||
25983|Labouchere Formation|29663|2|Defined|p53|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25983|Labouchere Formation|30010|4|Described|p45|||||||||
25983|Labouchere Formation|35975|3|Fully described|p103|||||||||
25983|Labouchere Formation|36551|6|Mentioned|Table 29|||||||||
25983|Labouchere Formation|37024|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25983|Labouchere Formation|37213|4|Described|p19|||||||||
25983|Labouchere Formation|37460|4|Described|p144|||||||||
25983|Labouchere Formation|39427|6|Mentioned|p5|||||||||
25983|Labouchere Formation|40937|6|Mentioned|p29|||||||||
25983|Labouchere Formation|40938|5|Briefly described|p11|||Mention P69||||||
25983|Labouchere Formation|40989|4|Described|p25|||||||||
25983|Labouchere Formation|42260|6|Mentioned|p125|||||||||
25983|Labouchere Formation|42730|5|Briefly described|Fig 12, P15|||||||||
25983|Labouchere Formation|43069|5|Briefly described|Fig.2|||of Glengarry Group||||||
25983|Labouchere Formation|43830|5|Briefly described|Map Legend||Paleoproterozoic|Padbury Basin||||||07-NOV-08
25983|Labouchere Formation|43831|5|Briefly described|Map Legend||Paleoproterozoic|Padbury Basin||||||07-NOV-08
25983|Labouchere Formation|44927|6|Mentioned|Map Legend|||||||||
25983|Labouchere Formation|49896|1|Redefined|p56 App. 3, p10|Paleoproterozoic|Paleoproterozoic|Prev. Labouchere Beds (MacLeod 1970). Variously interp. to be of Padbury Gp then Glengarry Gp; reassigned to Padbury Gp (Occhipinti et al 1997). Underlies Wilthorpe Fm; unconformable on Horseshoe Fm in type area. Max.thick: 4000m. See also p2 Tb. 1, p3 Tb. 2||||||01-JUL-13
25983|Labouchere Formation|50222|5|Briefly described|p320 Fig. 3, p327|Paleoproterozoic|Paleoproterozoic|Of the Padbury Group.  Max. thickness: 4000m.  Geological Province: Padbury Basin.||||||07-NOV-08
25983|Labouchere Formation|61271|6|Mentioned|p106|||Of the Padbury Group.||||||
25983|Labouchere Formation|62289|6|Mentioned|p4 Fig. 2|Palaeoproterozoic|Palaeoproterozoic|Padbury Group, Padbury Basin.||||||
25983|Labouchere Formation|63866|5|Briefly described|p164, p175|Orosirian|Orosirian|Western Glengarry Basin.|2000-1900 Ma (Windh, 1992)|Padbury Group||||
25983|Labouchere Formation|64384|5|Briefly described|p78 Tb. 8|||Top unit of the Glengarry Group. Geological province: Glengarry Sub-basin. Sandstone rocks.||||||07-FEB-11
25983|Labouchere Formation|64580|4|Described|map legend||Paleoproterozoic|Of Padbury Group. Quartz arenite; minor interleaved quartz wacke and siltstone; local quartz pebble conglomerate layers; turbiditic.||||||09-DEC-08
25983|Labouchere Formation|65408|5|Briefly described|p83, p85|Paleoproterozoic|Orosirian|Age based on youngest detrital zircons, but also said to overlie Bryah Group.|2.0 - 1.9 Ga maximum deposition age (Windh 1992)|Unit in Padbury Group.|||Turbidite sequence: quartz wacke, siltstone.|18-NOV-11
25983|Labouchere Formation|65411|5|Briefly described|p88, p90, p91.|Paleoproterozoic|Paleoproterozoic|||Basal unit in Padbury Group.|||Regularly layered quartz wacke, siltstone; regionally extensive quartzarenite marker bed; local quartz-muscovite-biotite-staurolite schist.|
25983|Labouchere Formation|65419|1|Redefined|p30, p36, pp37-40.|Paleoproterozoic|Paleoproterozoic|Named after Mount Labouchere, the type area. Composite type section is described. Thickness c.4000 m. Includes strata referred to as the Labouchere Beds by MacLeod (1970), Labouchere Formation (Barnett 1975; Gee 1979,1987; Elias and Williams 1980; and Martin 1994). Included in the Bryah Group by Pirajno and Occhipinti (1995), but re-assigned to the Padbury Group in this study. Maximum depositional age from detrital zircons.|2.0 - 1.9 Ga (Nutman in Windh, 1992)|Basal unit in Padbury Group.||Overlies Horseshoe Formation unconformably, but locally conformably. Is faulted against Despair Granite. Is overlain conformably by Wilthorpe Formation.|Quartz arenite, quartz wacke, siltstone, minor conglomerate and banded iron-formation in upward-coarsening successions.|
25983|Labouchere Formation|65896|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in lower Padbury Group. Metamorphosed quartz wacke, siltstone and shale; zones of pervasive foliation comprising quartz-mica schists; locally with staurolite and andalusite porphyroblasts; locally with metamorphosed banded iron formation.||||||
25983|Labouchere Formation|66112|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Padbury Group. Quartz wacke and siltstone with local quartz pebble conglomerate beds. Zones of quartz schist, quartz-muscovite schist, and minor biotite-muscovite schist, locally with chloritoid, staurolite and/or andalusite. ||||||
25983|Labouchere Formation|67246|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Padbury Basin.|1983 - 1811 Ma.|Unit in Padbury Group.||Intruded by Moorarie Supersuite. Is overlain unconformably by Yilgatherra Formation.|Quartz wacke and siltstone with local quartz-pebble conglomerate beds; metamorphosed; includes zones of quartz schist, quartz-muscovite schist, and minor biotite-muscovite schist, locally with chloritoid, staurolite and/or andalusite.|
25983|Labouchere Formation|67855|5|Briefly described|p204 tab 3-1|Paleoproterozoic|Paleoproterozoic|Gascoyne Complex, Nabberu Basin. 2km thick iron formation-sandstone-shale basin-fill facies||Glengarry Group||||
25983|Labouchere Formation|67888|6|Mentioned|p54|||||Padbury Group||||
25983|Labouchere Formation|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic|||Padbury Group|||Quartz arenite; minor interleaved quartz wacke and siltstone; Quartz wacke and siltstone; local quartz pebble conglomerate layers; turbiditic.|
25983|Labouchere Formation|69003|5|Briefly described|p16|||Padbury Basin, Capricorn Orogen. Deep-water turbidites.||Padbury Group.||Is overlain conformably by Wilthorpe Formation.|Mainly turbidites; lesser shale, siltstone.|
25983|Labouchere Formation|69010|5|Briefly described|Map Legend|Statherian|Orosirian|Padbury Basin. An unnamed sub-unit, of metamorphosed quartz arenite with minor interleaved quartz wacke and siltstone, is mapped separately.|1983-1620 Ma|Of the Padbury Group.|||Comprises quartz wacke and siltstone with local quartz-pebble conglomerate beds; including quartz schist, quartz-muscovite schist, and minor biotite-muscovite schist, locally with chloritoid, staurolite, and/or andalusite.|24-APR-14
25983|Labouchere Formation|69028|5|Briefly described|Map Legend|Orosirian|Orosirian|Padbury Basin.||Of the Padbury Group.||Is overlain by Wilthorpe Formation.|Quartz wacke and siltstone with local quartz-pebble conglomerate; metamorphosed; includes quartz schist, quartz-muscovite schist, and minor biotite-muscovite schist, locally with chloritoid, staurolite, and/or andalusite.|06-MAY-14
25983|Labouchere Formation|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|||Padbury Group|||Quartz arenite; minor interleaved quartz wacke and siltstone with minor fine grained sandstone and local quartz-pebble conglomerate beds. Quartz schist, quartz-muscovite schist and minor biotite-muscovite schist.|
25983|Labouchere Formation|69596|5|Briefly described|p10-11|||Padbury Basin.|||||Upward-coarsening, deep-water turbidites.|
25983|Labouchere Formation|70795|5|Briefly described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_geologyl_lut.csv, 100k_geologysub_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, West Australian Craton, Padbury Formation|1983-1811 Ma|||Overlain by Yilgatherra Formation, unconformably overlain by Edmund Group, Intruded by Moorarie Supersuite|Quartz wacke and siltstone with local quartz pebble conglomerate beds; quartz arenite. Sandstone, chert, banded iron formation and ferruginous chert; metamorphosed.|
25983|Labouchere Formation|70796|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|Padbury Basin, Capricorn Orogen.|1983 +/ 12 Ma to 1811 +/ 5 Ma (isotopic)|Padbury Group|||Quartz wacke and siltstone with local quartzpebble conglomerate beds; includes quartz schist, quartzmuscovite schist, and minor biotitemuscovite schist, locally with chloritoid, staurolite, and/or andalusite.|
25983|Labouchere Formation|70804|4|Described|p2-p3, p8, p17-p18|Early Proterozoic|Early Proterozoic|Outcrops in the northwest Bryah Basin where it is faulted against the Yarlarweelor gneiss complex. Outcrop extends from Mount Labouchere on MILGUN (where the type area of Martin, 1994 is found) to the Horseshoe Range. The type section of Martin a composite stratigraphy (up to 7km thick) based on four seperate sections in southeastern Milgun. Gee (1979) estimated a maximum thickness of this unit of 5000m. Petrography and lithology discussed in detail. See also p24-p26, p30, p42, plate 1.||Padbury Group||Unconformably overlies the Horseshoe Formation. Conformably (gradationally) overlain by the Wilthorpe Formation.|Quartz arenite, medium- to coarse-grained sericitic quartz wacke and sericitic siltstone, minor conglomerate and banded iron formation.|
25983|Labouchere Formation|70814|5|Briefly described|p48|||Padbury Basin. An economic gold deposit occurs at the contact between this formation and an unnamed gabbro body.||Padbury Group|||Metamorphosed sandstone and siltstone.|
25983|Labouchere Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||greywacke, shale, conglomerate, sandstone, banded iron formation|28-FEB-23
25983|Labouchere Formation|71269|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Of Padbury Basin. Events: Capricorn Orogeny (1817-1772 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 1m_geologyl12_lut.csv.|1983+\-12 Ma; 1811+\-5 Ma (isotopic)|Unit of Padbury Group.|||Quartz wacke and siltstone with local quartz-pebble conglomerate beds; includes quartz schist, quartz--muscovite schist, and minor biotite--muscovite schist, locally with chloritoid, staurolite, and/or andalusite|
25983|Labouchere Formation|71484|4|Described|p125,129,134-137|Orosirian|Orosirian|Geological province: Of Padbury Basin. Primary mineral constituents have been metamorphosed to quartz, sericite, and locally chlorite, forming quartz-sericite schists and chlorite-quartz schists. Forms a 5000m thick turbidite complex with the Wilthorpe Formation that outcrops in the W Padbury Basin (Martin, 1998). Maximum depostional age constraint of c. 2030-1960 Ma coincides with 2000-1950 Ma Glenburgh Orogeny.||Unit of Padbury Group.||Overlain by Wilthorpe Formation. Underlain unconformably by Horseshoe Formation/Bryah Group.|Quartz wacke and siltstone with local quartz-pebble conglomerate beds.|30-AUG-19
25983|Labouchere Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Padbury Basin.|Max age 1983+/- 12 Ma, Min 1811+/-5 Ma.|Padbury Group|||Quartz wacke and siltstone with local quartz-pebble conglomerate beds; includes quartz schist, quartz-muscovite schist, and minor biotite-muscovite schist, locally with chloritoid, staurolite, and/or andalusite.|
28661|Lacey Creek Formation|39210|6|Mentioned|p48|||||||||
34375|Lacuna Supersequence|22682|5|Briefly described|Fig20,p29|Siderian|Archean|2543-2499 Ma. Hamersley Province. Previously part of the Brockman Supersequence||||||03-MAR-10
39511|Lady Adelaide Orthogneiss|63417|5|Briefly described|Map legend|Archean|Archean|Of the Tambina Supersuite. Geological Province: Pilbara Craton. Orthogneiss after granodiorite; leucocratic; fine- to medium-grained.||||||07-NOV-08
39511|Lady Adelaide Orthogneiss|63441|5|Briefly described|p7 Tb. 2|Archean|Archean|Of the Tambina Supersuite. Geological province: Pilbara Craton.||||||07-FEB-11
39511|Lady Adelaide Orthogneiss|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||Of Mount Edgar Granitoid Complex.|||Orthogneiss after monzogranite; leucocratic, fine- to medium-grained.|
39511|Lady Adelaide Orthogneiss|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c.3435 - 3430 Ma.|Of Tambina Supersuite.|||Orthogneiss derived from granodiorite; leucocratic; fine- to medium-grained.|
39511|Lady Adelaide Orthogneiss|65827|2|Defined|p6 Tb.2, p9 Fig 3, p20, p46, p59|Paleoarchean|Paleoarchean|New name. Type area is a creek section 1 km west of Lady Adelaide gold mine. NE-trending lenticular body, 3.5 km x 500 m. <3430Ma, >3314Ma (inferred). Wrongly attributed to Emu Pool Supersuite on p59.  Hosts gold-bearing quartz veins.||Of Tambina Supersuite.||Intruded Duffer Formation, Underwood Gneiss and Fig Tree Gneiss.|Leucocratic biotite- and muscovite-bearing, quartzofeldspathic orthogneiss, strong gneissic fabric; the protolith was probably granodiorite to tonalite in composition; lacks mafic xenoliths and dykes.|21-MAY-14
39511|Lady Adelaide Orthogneiss|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Tambina Supersuite|||Gneissose leucocratic metagranodiorite; homogeneous to schlieric-textured|
39511|Lady Adelaide Orthogneiss|69566|6|Mentioned|p236|||Mount Edgar Granitoid Complex, East Pilbara Granite-Greenstone Terrane.||Tambina Supersuite.||||
39511|Lady Adelaide Orthogneiss|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3459-3410 Ma (inferred)|Unit of Tambina Supersuite.|||Gneissose leucocratic metagranodiorite; homogeneous to schlieric-textured|
39511|Lady Adelaide Orthogneiss|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|||Tambina Supersuite|||Gneissose leucocratic metagranodiorite; homogeneous to schlieric-textured.|
74873|Lady Alma Igneous Complex|64891|5|Briefly described|p37 Fig. 2, p38, p43, p50-51 Tb. 1|Archean|Archean|Of the Meeline Suite. Ages:2821+/-5Ma, 2810+/-5Ma and 2815+/-7Ma (zircon form gabbro) - but these zircon ages are older than interpreted host rock age and are therefore, probably inherited zircons. Geol.prov: Murch.Dom. Layered gabbro/anorthosite, etc.||||||07-FEB-11
74873|Lady Alma Igneous Complex|66195|4|Described|p604, 605, p598, p599 Fig.2, p602|Neoarchean|Mesoarchean| >1km thick. U-Pb age of zircon from gabbro (zircons may be inherited). Divided into lower zone (~1km thick) and upper zone (~200m thick). See figure 4 for more detail. Has upper contact with Norie Group felsic supracrustal rocks.|2821 +/- 5 Ma.|In Meeline Suite.|||Has significant magnetitite horizons.|13-MAR-12
74873|Lady Alma Igneous Complex|67129|5|Briefly described|p18 Fig.19, p52, p54-55|Archean|Archean|Murchison Domain, Youanmi Terrane.|2821 +/- 5 Ma.|Meeline Suite.||||
74873|Lady Alma Igneous Complex|68110|5|Briefly described|p672 Fig.1, p673, p675|Neoarchean|Mesoarchean|South of Meekatharra. Appears as Lady Alma Complex on p673. Cumulate ultramafic rocks with low TiO2 contents.|2821 +/- 5 Ma||||Structurally-dismembered mafic-ultramafic layered intrusion.|
74873|Lady Alma Igneous Complex|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane||Meeline Suite|Includes informal Gabanintha metagabbro and 5 unnamed subunits.||Peridotitic schist; Magnetitite; Pyroxenite; Gabbro; Leucogabbro to gabbroic anorthosite;|
74873|Lady Alma Igneous Complex|69583|5|Briefly described|p49-50, p98, p102, p177; Plate 2|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Igneous stratigraphic column.|<2821 Ma.||||Gabbro with local leucogabbro; metamorphosed.|
74873|Lady Alma Igneous Complex|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean|||Meeline Suite||||
74873|Lady Alma Igneous Complex|69586|5|Briefly described|p22|Mesoarchean|Mesoarchean|Murchison Domain.||Meeline Suite.||||
74873|Lady Alma Igneous Complex|69628|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. The four facies are mapped separately.||Meeline Suite|||Leucogabbro to gabbroic anorthosite, medium to coarse grained, metamorphosed; magnetitite fine to coarse grained, metamorphosed; peridotitic schist, serpentine-chlorite-actinolite; pyroxenite, massive to weakly foliated, metamorphosed.|
74873|Lady Alma Igneous Complex|70419|5|Briefly described|p7-8|||Between 3 to 5 km thick; has distinctive magnetitite units in its upper zone.|<2821 Ma (Wang, 1998).|Meeline Suite.||||
74873|Lady Alma Igneous Complex|70796|5|Briefly described|100k_interpgeol_lut.csv,|Mesoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. See also 100K_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 194747.1.pdf, 194751.1.pdf, Nowthanna100_2643_stratig.pdf. Numerous additional lithologies are discussed.|ca 2813 Ma (inferred)||||Fine to coarse grained magnetite; metamorphosed. Medium to coarsegrained gabbro with local leucogabbro. Leucogabbro to gabbroic anorthosite, pyroxenite and peridotite schist.|
74873|Lady Alma Igneous Complex|70830|5|Briefly described|p4, p27||||<2821 Ma (Wang, 1998)|Meeline Suite||||
74873|Lady Alma Igneous Complex|71168|5|Briefly described|p7, p18, p22|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c. 2800 Ma|Meeline Suite||||
74873|Lady Alma Igneous Complex|71311|6|Mentioned|p794|||Northern Youanmi Terrane, Yilgarn Craton.||||||
74873|Lady Alma Igneous Complex|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Youanmi Terrane.|||||Gabbro; medium to coarse grained; local leucogabbro; metamorphosed.|
74873|Lady Alma Igneous Complex|72389|5|Briefly described|Map Legend|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Gabanintha 1:100k map sheet 2644. Includes numerous unnamed constituents.||Meeline Suite|||Layered gabbro and anorthosite with magnetite and pyroxenite layers and thick ultramafic cumulates; metamorphosed.|28-AUG-20
74873|Lady Alma Igneous Complex|72491|6|Mentioned|p5 Fig.4, p55|||Murchison Terrane, Yilgarn Craton. On p55, it is referred to as ""the Windimurra and Lady Alma mafic-ultramafic igneous complexes"". High-grade hornfelses were produced in their aureoles at 2825-2815 Ma.||||||
74873|Lady Alma Igneous Complex|73596|6|Mentioned|p1161, 1170|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane.|2821 +/- 5 Ma.|Norie Group.|||Mafic-ultramafic layered igneous complex.|
33912|Lagoon rhyolite|22449|6|Mentioned|Table3 P27||Archean|Age of unit is 3000 Ma.||||||07-NOV-08
74632|Lagrange Calcilutite Member|64449|2|Defined|p75|Holocene|Holocene|Of Sandfire Calcilutite. Consists of white/cream/grey bioturbated (locally laminated) calcilutite; underlies salt flats, samphire flats, and mangrove flats.||||||07-FEB-11
74632|Lagrange Calcilutite Member|73213|5|Briefly described|958 Fig.3(a)|||||Sandfire Calcilutite.||Overlies Djugun Member and Crab Creek Calcilutite Member. Is locally overlain by Race Course Plains Coquina.||
67868|Lake Brazier Tonalite|60076|5|Briefly described|p46 App. 1|||[Agtlb]   Highly variable biotite- and hornblende-bearing tonalite to granodiorite.||||||
67868|Lake Brazier Tonalite|65258|5|Briefly described|Map Legend|Archaean|Archaean|Highly variable biotite and hornblende-bearing tonolite to granodiorite.||||||16-JUN-09
67868|Lake Brazier Tonalite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Highly variable biotite- and hornblende-bearing tonalite to granodiorite.||||||07-FEB-11
67868|Lake Brazier Tonalite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Biotite- and hornblende-bearing tonalite to granodiorite.|06-AUG-15
67868|Lake Brazier Tonalite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Biotite- and hornblende-bearing tonalite to granodiorite.|
67868|Lake Brazier Tonalite|70802|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton.|||||Biotite- and hornblende-bearing tonalite to granodiorite|
67868|Lake Brazier Tonalite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||tonalite, granodiorite|
67868|Lake Brazier Tonalite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. See 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|||||Biotite- and hornblende-bearing tonalite to granodiorite|
34482|Lake Deborah Formation|22769|6|Mentioned|p759|||||||||
77927|Lake Douglas Conglomerate Member|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|The rank of Member was omitted.|2657 +/- 7 Ma (isotopic) - 2640 Ma (inferred).|Kurrawang Formation|||Lower unit: conglomerate, sandy conglomerate, and pebbly sandstone; metamorphosed.|
67870|Lake Dundas Monzogranite|60076|5|Briefly described|p45 App. 1|||[Agmld]   Subequigranular, medium- to coarse-grained biotite monzogranite.||||||
67870|Lake Dundas Monzogranite|65258|5|Briefly described|Map Legend|Archaean|Archaean|Sub-equigranular, medium- to coarse-grained biotite monzogranite.||||||16-JUN-09
67870|Lake Dundas Monzogranite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Medium- to coarse-grained, equigranular biotite monzogranite.||||||07-FEB-11
67870|Lake Dundas Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Medium- to coarse-grained, equigranular biotite monzogranite.|06-AUG-15
67870|Lake Dundas Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Medium- to coarse-grained, equigranular biotite monzogranite.|
67870|Lake Dundas Monzogranite|70802|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton.|||||Medium- to coarse-grained, equigranular biotite monzogranite|
67870|Lake Dundas Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
67870|Lake Dundas Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. See 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|||||Medium- to coarse-grained, equigranular biotite monzogranite|
75544|Lake Mackay Quartzite|68994|4|Described|p4, p6-11, p14, p20, p24, p26-27|||Aileron Province. Conservative max depositional ag., Detrital zircon U-Pb ages listed and Hf analyses detailed. Also written as MacKay Quartzite and/or Lake MacKay Quartzite on p20 and p26.|1775+/-7 Ma (Kirkland et al. 2009).|||Overlies Dwarf Well Granite (Carrington Suite).|Deformed and recrystallised quartzite.|13-JAN-17
75544|Lake Mackay Quartzite|69031|5|Briefly described|p4, p6 Fig.4, p7, p26|||Aileron Province, Arunta Orogen. Detrital zircon age data.|1750 +/- 19 Ma (maximum depositional age).|||Nonconformably overlies Dwarf Well Granite. May correlate with Reynolds Range Group.|Deformed and strongly recrystallised quartzite.|
75544|Lake Mackay Quartzite|70826|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|||||||
75544|Lake Mackay Quartzite|71348|5|Briefly described|p217|Paleoproterozoic|Paleoproterozoic|Geological province: Aileron Province, Arunta Region. Maximum depositional age c. 1780 Ma (Hollis et al., 2013; Scrimgeour, 2013; Rosel et al.,2014).|< 1780 Ma.|||Underlain unconformably by Lander Rock Formation.||
75544|Lake Mackay Quartzite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Orogen.|||||Interbedded quartzite and quartz--mica schist.|
77851|Lake Medcalf Igneous Complex|68520|5|Briefly described|Map legend|Archean|Archean|Southern Cross Domain, Youanmi Terrane, Yilgarn Craton. The 2 facies variants are mapped separately.|||||Pyroxenite, metamorphosed; amphibolite after gabbro and dolerite, minor metamorphosed leucogabbro and pyroxenite.|
77851|Lake Medcalf Igneous Complex|69404|5|Briefly described|p8|||Lake Johnston greenstone belt. ||||Intrudes the Maggie Hays Formation|Dolerite dykes, quartzofeldspathic sills, and mafic to ultramafic intrusive rocks.|
77851|Lake Medcalf Igneous Complex|69559|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean|Southern Cross Domain, Youanmi Terrane, Yilgarn Craton. See also 100k_interpgeol_lut.csv, geologyp_lut.csv,  500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv,  geologyl_lut.csv.|2873-2720 Ma||||Amphibolite after gabbro and dolerite; minor metamorphosed leucogabbro and pyroxenite.|
77851|Lake Medcalf Igneous Complex|69617|5|Briefly described|p145-148, p154-155|||Lake Johnston greenstone belt, Youanmi Terrane, Yilgarn Craton. Concordant, sill-like intrusions.||||Intrudes Maggie Hays Formation; underlies Honman Formation.|Medium- to coarse-grained metapyroxenite to metaleucogabbro and meta-anorthosite; medium-to coarse-grained metagabbro; typically highly strained.|
77851|Lake Medcalf Igneous Complex|70144|5|Briefly described|Map legend|Archean|Archean|Southern Cross Domain, Youanmi Terrane, Yilgarn Craton.|||||Amphibolite after gabbro and dolerite; minor metamorphosed leucograbbro and pyroxenite.|
77851|Lake Medcalf Igneous Complex|70205|5|Briefly described|Map legend.|Archean|Archean|Southern Cross Domain, Youanmi Terrane, Yilgarn Craton. The two facies are mapped separately.|||||Amphibolite after gabbro and dolerite; minor metamorphosed leucogabbro and pyroxenite. Metamorphosed dolerite.|
77851|Lake Medcalf Igneous Complex|70794|5|Briefly described|100k_geologyp_lut.csv|Neoarchean|Mesoarchean|Youanmi Terrane, Yilgarn Craton. Age range 2873-2720 Ma shown in 500k_interpgeop14_lut.csv. See also  500k_interpgeop_lut.csv.|2920-2718 Ma inferred||||Amphibolite after gabbro and dolerite; minor metamorphosed leucogabbro and pyroxenite.Dolerite; metamorphosed. Gabbro with minor dolerite; metamorphosed.|
77851|Lake Medcalf Igneous Complex|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Mesoarchean|Youanmi Terrane.|||||Gabbro with minor dolerite; metamorphosed.|
35819|Lake Willson beds|23314|5|Briefly described|336|Mesoproterozoic|Mesoproterozoic|||||||06-JAN-10
35819|Lake Willson beds|65074|4|Described|p349, p351 fig 4-37, p352-353, p362|Mesoproterozoic|Mesoproterozoic|See also p355 Tb. 4-11. Of NW Birrindudu Basin. 150m thick. Spelt Lake Wilson on p351. Reference area details given.||||Probably equivalent to Talbot Well Formation. Conformably overlain by Pindar beds.|Flat-lying stromatolitic chert.|
35819|Lake Willson beds|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Shallow marine stromatolitic chert, medium grained cross bedded sublithic sandstone siltstone and shale|
79814|Lakeside Complex|69586|5|Briefly described|p31 Fig.33|||Constitutes the Lakeside Pluton [not a stratigraphic name] in the Mount Magnet area.|||||Porphyritic monzogranite, schlieren monzogranite, leucogranite, mylonitic monzogranite and leucogranite.|
79814|Lakeside Complex|71311|5|Briefly described|p794-795, p801|||Van Kranendonk and Ivanic (2009). Northern Youanmi Terrane, Yilgarn Craton. The authors confusingly use the term Lakeside complex for an informal structural granite-gneiss complex, unrelated to the stratigraphic name; it is accordingly not indexed.|||||Leucogranite, mylonitic leucogranite, monzogranite: equigranular and/or porphyritic, schlieren monzogranite, porphyritic monzogranite and leucogranite, porphyritic and schlieren monzogranite.|
80132|Lakeside Granite|69583|5|Briefly described|p94, p113, p119-121, p151, p174|||Near the W margin of the Mount Magnet greenstone belt. Adjacent to the synmagmatic Wattle Creek Shear Zone. See also Lakeside granite (p42, p44), Lakeside pluton p116.|c.2700 Ma emplacement age.||||Tonalite to monzogranite.|27-SEP-17
73566|Lakeside Limestone Member|63454|4|Described|p76|Late Pleistocene|Late Pleistocene|Upper part of Kooallup Limestone. Aeolianites; cross-laminated to structureless, fine and medium calcarenite. Type location is same as for the formation. see also Lakeside Member.||||||
79815|Lakeside granite|69583|6|Mentioned|p42, p44|||Large, composite pluton associated with migmatites; shows widespread evidence of deformation during and immediately after crystallisation. See also Lakeside Granite on p94, p113, p119-121, p151, p174.||||||
79815|Lakeside granite|69586|6|Mentioned|p7|||See also Lakeside Complex (p31 Fig.33).||||||
79815|Lakeside granite|69744|5|Briefly described|p255-265|||Murchison Domain, Youanmi Terrane. c.100km x 50km. More commonly referred to as the Lakeside Pluton. Photographs. Geochemistry elaborated. Age also given as ~2705-2690 Ma. Progressively assembled by coalescence of 1-10m-thick sheets. Widespread deformation developed during pluton emplacement.|c.2710-2695 Ma.||||Composite syntectonic pluton associated with migmatites. Mainly monzogranitic in composition, with subordinate trondhjemitic to granodioritic rock types. Amphibolite and tonalite xenoliths (detailed).|
28108|Lalla Rookh Sandstone|22715|5|Briefly described|table7 p214|Archean|Archean|Age: 3000Ma.||||||07-NOV-08
28108|Lalla Rookh Sandstone|23134|5|Briefly described|p288||Archean|Of the De Grey Group.||||||07-NOV-08
28108|Lalla Rookh Sandstone|23255|6|Mentioned|Fig.2|||||||||
28108|Lalla Rookh Sandstone|23416|5|Briefly described|Map Legend|Archean|Archean|Of De Grey Group, Pilbara Craton||||||07-NOV-08
28108|Lalla Rookh Sandstone|23755|4|Described|p45|Archean|Archean|See also page 17 table 1.  Of De Grey Group.||||||07-NOV-08
28108|Lalla Rookh Sandstone|23783|5|Briefly described|p41|Archean|Archean|Of De Grey Group.  Age: 2940Ma.||||||07-NOV-08
28108|Lalla Rookh Sandstone|23793|6|Mentioned|p6|||||||||
28108|Lalla Rookh Sandstone|23807|6|Mentioned|p141|||Geological Province: Pilbara Craton.||||||
28108|Lalla Rookh Sandstone|23895|5|Briefly described|p885 Fig.5, 887 Fig.3|||Geological Province: Pilbara Craton.||||||07-MAR-05
28108|Lalla Rookh Sandstone|23936|5|Briefly described|p3|||Geoological Province: Pilbara Craton. Parent: De Grey Group.||||||
28108|Lalla Rookh Sandstone|24025|4|Described|p8 Tb. 1|Archean|Archean|Of De Grey Group.  Max. thickness: 5000m. Conglomerate, sandstone minor shale.  Geological Province: Pilbara Craton.||||||07-NOV-08
28108|Lalla Rookh Sandstone|24110|5|Briefly described|Plate 1|Archean|Archean|Parent: De Grey Group.  Geological Province: Pilbara Craton||||||07-NOV-08
28108|Lalla Rookh Sandstone|24531|5|Briefly described|p23|Archean|Archean|Of the De Grey Group (Pilbara Supergroup). Geological Province: Pilbara Craton. See also p5 Table 1.||||||07-NOV-08
28108|Lalla Rookh Sandstone|24532|5|Briefly described|Map legend|Archean|Archean|Of the De Grey Group.||||||07-NOV-08
28108|Lalla Rookh Sandstone|24550|5|Briefly described|p31 Tb. 3.1|Archean|Archean|Of the De Grey Group. Sandstone, conglomerate, shale. Age: ca 2950Ma. Geological Province: Pilbara Craton.||||||07-FEB-11
28108|Lalla Rookh Sandstone|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Of the De Grey Group. Conglomerate, sandstone, minor shale. Age: 2950-2930Ma. See also p75, p84 Fig. 3.3.||||||07-FEB-11
28108|Lalla Rookh Sandstone|30766|6|Mentioned|p13|||||||||
28108|Lalla Rookh Sandstone|31853|2|Defined|p62|Archean|Archean|||||||07-NOV-08
28108|Lalla Rookh Sandstone|37373|4|Described|p79|||||||||
28108|Lalla Rookh Sandstone|38498|4|Described|p61|||See also Table 1.||||||
28108|Lalla Rookh Sandstone|38544|6|Mentioned|Fig.1|||||||||
28108|Lalla Rookh Sandstone|39426|6|Mentioned|p3|||||||||
28108|Lalla Rookh Sandstone|39444|6|Mentioned|Table 1|||||||||
28108|Lalla Rookh Sandstone|39697|3|Fully described|p101|||||||||
28108|Lalla Rookh Sandstone|41252|6|Mentioned|p49|||||||||
28108|Lalla Rookh Sandstone|41353|4|Described|p72|||||||||
28108|Lalla Rookh Sandstone|41354|5|Briefly described|p90|||||||||
28108|Lalla Rookh Sandstone|41355|5|Briefly described|p114|||||||||
28108|Lalla Rookh Sandstone|41635|4|Described|p21|||||||||
28108|Lalla Rookh Sandstone|42231|4|Described|p335|||||||||
28108|Lalla Rookh Sandstone|43595|5|Briefly described|p213|||||||||
28108|Lalla Rookh Sandstone|43698|6|Mentioned|p26|||||||||
28108|Lalla Rookh Sandstone|44150|5|Briefly described|p129 Tb.2-15, p132 Fig.2-131, p135-136|||See also p152 Tb.2-22, p157 Fig.2-144. Thickness 3-5km.||Gorge Creek Group|||Sandstone, quartzite and conglomerate. Dominated by well-sorted, slightly feldspathic, cross-bedded sandstone.|
28108|Lalla Rookh Sandstone|50189|5|Briefly described|p18|Archean|Archean|Once included in the De Grey Group. Epiclastic rocks correlated with the Whim Creek Group.||||||07-NOV-08
28108|Lalla Rookh Sandstone|50427|5|Briefly described|p198 Fig.14|Archean|Archean|Of De Grey Group.||||||07-NOV-08
28108|Lalla Rookh Sandstone|60429|5|Briefly described|p18|||Formerly of the Gorge Creek Group, these rocks are now reassigned to De Grey Group as two new formations: Cattle Well and Coora Goora Formations. Epiclastic rocks.||||||07-FEB-11
28108|Lalla Rookh Sandstone|61252|5|Briefly described|p65|||Unconformably overlain by Mount Roe Basalt. Reference to the "Lalla Rookh Basin" is deemed incorrect by the authors, since the sandstone occurs over most of NORTH SHAW.||||||
28108|Lalla Rookh Sandstone|61253|5|Briefly described|p56, p52 Fig. 2|Archean|Archean|Of the Goldsworthy Group (Pilbara Supergroup) - which are eroded and deformed remnants of the De Grey Supergroup.  Geological Province: eastern Pilbara Craton.||||||07-NOV-08
28108|Lalla Rookh Sandstone|61264|5|Briefly described|p63 Fig. 1|Archean|Archean|Of the De Grey Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
28108|Lalla Rookh Sandstone|61266|4|Described|p58 Tb.1, p61|Archean|Archean|Of the De Grey Group. Age: ca. 2950 Ma (Van Kranendonk and Collins, 1998). Unconformably overlain by the Mount Roe Basalt. Conglomerate, sandstone, minor shale. Geological Province: Pilbara Craton.||||||07-NOV-08
28108|Lalla Rookh Sandstone|61579|5|Briefly described|p58 Fig. 2|Archean|Archean|Of the De Grey Group. Age: c.2950Ma. ||||||07-NOV-08
28108|Lalla Rookh Sandstone|63420|5|Briefly described|Map legend|Archean|Archean|Of the Croydon Group (De Grey Supergroup). Overlain by Bellary Formation or Mount Roe Basalt. Geological Province: Lalla Rookh Basin/Pilbara Craton. Chert and banded iron formation, minor felsic volcaniclastic rock, shale and siltstone; metamorphosed.||||||07-NOV-08
28108|Lalla Rookh Sandstone|63441|5|Briefly described|p5 tb. 1, p29|Archean|Archean|Of Croydon Gp (Pilbara Supergp). Unconformable on Honeyeater Basalt + Pyramid Hill Fm (Soanesville Gp).Thickness:>3000m.Geol.prov: Mallina Basin. Thick succession of mainly coarse pebble conglomerate and sandstone + lesser siltstone and mudstone higher up||||||07-FEB-11
28108|Lalla Rookh Sandstone|63538|4|Described|p6 Fig. 3|Archean|Archean|In figure, Sandstone is spelt Sst. Of Croydon Group. Underlain by Cattle Well Formation. Geological Province: Pilbara Craton. Sedimentary rocks.||||||19-APR-13
28108|Lalla Rookh Sandstone|63854|6|Mentioned|p228 Fig.1, p230|||East Pilbara Terrane.||Unit in De Grey Supergroup.||||
28108|Lalla Rookh Sandstone|64328|5|Briefly described|p56 Tb. 1|||Of the De Grey Group.||||||07-FEB-11
28108|Lalla Rookh Sandstone|64384|5|Briefly described|p26 Tb. 3|Archean|Archean|Of the Gorge Creek Group. Max. thickness: 500m.||||||07-FEB-11
28108|Lalla Rookh Sandstone|64580|4|Described|map legend||Mesoarchean|Of Croydon Group. Sandstone containing conglomerate, and minor siltstone and shale; metamorphosed.||||||15-DEC-08
28108|Lalla Rookh Sandstone|64621|5|Briefly described|Map legend|Archean|Archean|Of Croydon Group (De Grey Supergroup). Sandstone with beds of conglomerate, and minor siltstone and shale; metamorphosed.||||||07-NOV-08
28108|Lalla Rookh Sandstone|64936|5|Briefly described|map legend|Archean|Archean|Of De Grey Group. Unconformable under Bellary Formation; over Paddy Market Formation. Conglomerate and sandstone; shale; sandstone, with minor conglomerate and siltstone. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
28108|Lalla Rookh Sandstone|65008|6|Mentioned|p2|||||Of the De Grey Group||||
28108|Lalla Rookh Sandstone|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Lalla Rookh Basin, in De Grey Superbasin. Unit in Croydon Group. Sandstone with beds of conglomerate, and minor siltstone and shale; metamorphosed.||||||11-APR-13
28108|Lalla Rookh Sandstone|66118|4|Described|p148|||Pilbara Craton|c. 2940 Ma|De Grey Supergroup||Unconformably overlies Pyramid Hill Formation.||
28108|Lalla Rookh Sandstone|66217|4|Described|p1, p39, pp42-44.|Mesoarchean|Mesoarchean|Lalla Rookh Basin, East Pilbara Terrane, Pilbara Craton. Up to 2000 m thick. Syn-orogenic deposition. Deformed at 2950-2930 Ma.|2.97-2.94 Ga.|Unit in Croydon Group.||Unconformably overlies Pilbara Supergroup and Gorge Creek Group. Is overlain unconformably by Fortescue Group.|Very coarse-grained polymictic basal conglomerates, overlain by interbedded sandstone and conglomerate, then interbedded shale, siltstone and sandstone.|
28108|Lalla Rookh Sandstone|67197|5|Briefly described|p9, p14, p19, p22, p29, p33-34, p36|||||Croydon Group.||Is faulted against Strelley Pool Formation.||
28108|Lalla Rookh Sandstone|67201|5|Briefly described|p7 Fig.4|||In northwestern Pilbara Craton, De Grey Superbasin, East Pilbara Terrane.||Croydon Group||||
28108|Lalla Rookh Sandstone|67269|5|Briefly described|p5|Paleoarchean|Paleoarchean|||Croydon Group.|||Sandstone and conglomerate.|
28108|Lalla Rookh Sandstone|68281|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Lalla Rookh Basin, De Grey Superbasin, Pilbara Craton. Detailed lithology discussed in map legend; 5 facies mapped separately.||Of the Croydon Group.|||Pebble to boulder conglomerate and interbedded coarse-grained sandstone; shale; minor siltstone; quartzose sandstone, thickly bedded; massive blue-grey conglomerate and breccia, siliceous matrix; all metamorphosed.|23-SEP-13
28108|Lalla Rookh Sandstone|68282|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Lalla Rookh Basin, De Grey Superbasin.||Of the Croydon Group|||Coarse-grained to pebbly sandstone and pebble conglomerate, minor siltstone and grey shale; pebble to boulder conglomerate and interbedded pebbly to coarse-grained sandstone; all metamorphosed.|03-DEC-14
28108|Lalla Rookh Sandstone|68283|5|Briefly described|Map Legend|Archean|Archean|Mallina and Lalla Rookh Basins.||Of the Croydon Group.|||Coarse-grained to pebbly sandstone and pebble conglomerate; minor siltstone and grey shale; metamorphosed.|23-SEP-13
28108|Lalla Rookh Sandstone|69015|5|Briefly described|Map Legend|Neoarchean|Mesoarchean|Lalla Rookh Basin, De Grey Superbasin. Mapped as 2 unnamed sub-units.||Of the Croydon Group.|||Pebble to boulder conglomerate and interbedded pebbly to coarse-grained sandstone; coarse-grained to pebbly sandstone and pebble conglomerate, minor siltstone and grey shale; all metamorphosed.|02-MAY-14
28108|Lalla Rookh Sandstone|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|Age derived from sample of feldspathic sandstone (142951.1.pdf) and constrains age of deposition of the sample.|3304 Ma +/- 6 Ma (SHRIMP)|Croydon Group|||Chert breccia, shale, coarse-pebbly sandstone and pebble conglomerate; metamorphosed. Sandstone, massive conglomerate, breccia and polymictic conglomerate interbedded with basaltic volcaniclastic rocks and ferruginous shale. Basaltic breccia.|
28108|Lalla Rookh Sandstone|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton. Of Budjan, Cattle Well, Goldsworthy, Lalla Rookh, and Mosquito Creek Basins.|< 3048-2941 Ma|Unit of Croydon Group.|||Sandstone containing conglomerate, and minor siltstone and shale; metamorphosed|
28108|Lalla Rookh Sandstone|69301|4|Described|p5 Fig.3, p15|||Pilbara Craton. East Pilbara Terrane. Mallina Basin.||Croydon Group||Overlies Cattle Well Formation.|Sedimentary rocks. Composed of fluviatile conglomerate, sandstone, and minor lacustrine shale.|
28108|Lalla Rookh Sandstone|69590|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton. Of Mallina and Lalla Rookh basins, De Grey Superbasin. Events: North Pilbara Orogeny. Sample GSWA 142951 (feldspathic sandstone) yielded an interpreted maximum depositional age of 3304+\-6 Ma (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|2948-2941 Ma (isotopic)|Unit of Croydon Group.|Includes Salt Well Member.||Massive, pebble to boulder conglomerate abd interbedded coarse-grained to pebbly sandstone, quartz sandstone, chert breccia; polymict chert clasts; turbidite and debris-flow deposits; includes basaltic breccia; metamorphosed.|
28108|Lalla Rookh Sandstone|70022|6|Mentioned|p115-116|||East Pilbara Terrane.|2.98-2.94 Ga.|Croydon Group.|||Feldspathic sandstone.|
28108|Lalla Rookh Sandstone|70775|4|Described|p11, p54-p55, p59, p64, p75|Mesoarchean|Mesoarchean|Previously incorporated into the De Grey Group, before being reassigned to the Croydon Group by Van Kranendonk et al. (2006). Hosts gold within conglomerate.|c. 3015-2940 Ma|Croydon Group|Includes the Salt Well Member.|Overlies the Cattle Well Formation and the Gorge Creek Group.|Sandstone and conglomerate.|
28108|Lalla Rookh Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, shale|
28108|Lalla Rookh Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mallina Basin.||Croydon Group|||Sandstone with beds of conglomerate, and minor siltstone and shale; metamorphosed.|
28108|Lalla Rookh Sandstone|72251|5|Briefly described|p54|Mesoarchean|Mesoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Croydon Group.||Overlain by Sisters Supersuite. Underlain by Cattle Well Formation.||
28108|Lalla Rookh Sandstone|72668|4|Described|p4, p14|||East Pilbara Terrane. Interpreted to have been deposited in a largely fluviatile environment changing to lacustrine setting towards the top of the formation. Deposition preceded or was contemporaneous with sinistral transpression at c. 2930 Ma.||||Overlies the Cattle Well Formation. Unconformably overlies the Pilbara Supergroup.|Coarse clastic rocks including sandstone.|13-JAN-22
28108|Lalla Rookh Sandstone|73598|6|Mentioned|p1212|Mesoarchean|Mesoarchean|East Pilbara Terrane.||Croydon Group.||Overlies Cattle Well Formation.||
33828|Lalla Rookh Supersequence|22546|4|Described|359|Archean|Archean|Geol. Province: Lalla Rookh Basin. Max thickness 3000 m. Age 3000 Ma to 2950 Ma||||||07-NOV-08
26272|Lambert Formation|23726|5|Briefly described|p8 Fig 2c|Eocene||Overlying unit Dockrell Formation. Geological Province: Carnarvon Basin.||||||
26272|Lambert Formation|40617|5|Briefly described|p16|||||||||
26272|Lambert Formation|40800|2|Defined|p12|Early Paleocene|Early Paleocene|||||||07-NOV-08
26272|Lambert Formation|41271|3|Fully described|p164|||||||||
26272|Lambert Formation|41437|6|Mentioned|p59|||||||||
26272|Lambert Formation|41439|6|Mentioned|p123|||||||||
26272|Lambert Formation|41732|6|Mentioned|Fig.3|||||||||
26272|Lambert Formation|42116|5|Briefly described|Fig.1 P6|||||||||
26272|Lambert Formation|43712|6|Mentioned|Fig.10,p52||Paleocene|||||||
26272|Lambert Formation|43724|6|Mentioned|Fig.15,p65||Paleocene|||||||
26272|Lambert Formation|61155|5|Briefly described|p15|Late Paleocene|Early Paleocene|Overlain by Dockrell Formation. Age: 64-62Ma. Max. thickness: 300m.  Geological Province: Carnarvon Basin /offshore.||||||
26272|Lambert Formation|62734|5|Briefly described|p1362 Fig. 2|Paleocene|Paleocene|Geological Province: Barrow Sub-basin.||||||01-SEP-08
26272|Lambert Formation|62837|5|Briefly described|Stratigraphic columns|Late Cretaceous|Late Cretaceous|Age: >65-60Ma. Geological Province: Dampier Sub-basin, Rankin Platform and Beagle Sub-basin.||||||
26272|Lambert Formation|63950|5|Briefly described|p336 Fig. 4|Paleocene|Paleocene|Partially overlies Miria Marl; underlies Dockrell Formation. Geological Province: northern Carnarvon Basin.||||||27-MAY-08
26272|Lambert Formation|67200|5|Briefly described|p8 fig 6, p53|Pliocene|Eocene|Thermal conductivity of 1.23 W/mK||||Overlain by Cardabia Calcarenite, Dockrell Formation|Crudely bedded limestone and marl.|
26272|Lambert Formation|67368|6|Mentioned|p209 Fig.4.|Paleocene|Paleocene|||||||
26272|Lambert Formation|67970|5|Briefly described|p25 Fig.4.|Selandian|Selandian|Exmouth Plateau.||||Is overlain by Dockerell Formation.||
26272|Lambert Formation|69692|6|Mentioned|p4|Paleocene|Paleocene|Northern Carnarvon Basin.||||Overlies Miria Marl. Is overlain by Dockrell Formation.||
26272|Lambert Formation|70066|5|Briefly described|Dampier: Fig.2. Exmouth: Fig.2|Selandian|Danian|See also Regional: Fig.6. Northern Carnarvon Basin.||||Overlies Miria Formation. Is overlain by Dockrell Formation and locally by Cardabia Calcarenite.||
80974|Lamboo Province granitic unit 80974|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Informal unit. Lamboo Province, Halls Creek Orogen. Age inferred.|||||Medium-grained leucocratic granite.|
34448|Lamboo Ultramafics|22754|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|Formerly Alice Downs Ultrabasics.||||||07-NOV-08
34448|Lamboo Ultramafics|23383|4|Described|p11, p5 Tb. 1|||Supersedes the Alice Downs Ultrabasics.  Of Lamboo Complex.  Intrudes Koongie Park Formation; intruded by Loadstone Monzogranite.  Geological Province: Halls Creek Orogen.  See also p6 Fig. 3.||||||25-JAN-05
34448|Lamboo Ultramafics|23599|5|Briefly described|p12|||Of the Lamboo Complex.||||||12-OCT-06
34448|Lamboo Ultramafics|23601|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Partly serpentinised ultramafic and mafic intrusive rocks.||||||07-NOV-08
34448|Lamboo Ultramafics|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: c.1835Ma.||||||07-NOV-08
34448|Lamboo Ultramafics|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Metamorphosed ultramafic- and mafic-intrusive rocks.||||||07-NOV-08
34448|Lamboo Ultramafics|44694|5|Briefly described|Map Legend||Proterozoic|Used as geological province.||||||
34448|Lamboo Ultramafics|64580|6|Mentioned|map legend|||Included in undivided mafic-ultramafic intrusions; may have interlayered metasedimentary rocks.||||||15-DEC-08
34448|Lamboo Ultramafics|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Metamorphosed ultramafic and mafic intrusives: metamorphosed peridotite, pyroxenite, gabbro, anorthosite, and amphibolite with interlayered medium grade metasediments|
34421|Lamil Group|22716|6|Mentioned|p237|Mesoproterozoic|Mesoproterozoic|||||||
34421|Lamil Group|22816|6|Mentioned|p2|||||||||
34421|Lamil Group|22907|6|Mentioned|40 fig 1|||||||||
34421|Lamil Group|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Yeneena Supergroup, Yeneena Basin.||||||
34421|Lamil Group|23414|5|Briefly described|Map Legend|Neoproterozoic|Mesoproterozoic|Of Yeneena Supergroup. geological province: Yenenna Basin.||||||25-JUL-07
34421|Lamil Group|23575|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Yeneena Supergroup.||||||
34421|Lamil Group|23585|5|Briefly described|p21|||Of Yeneena Supergroup. Underlain by Throssell Group. Geological Province: Yeneena Basin.||||||25-JUL-07
34421|Lamil Group|23590|4|Described|p9, p22 Appendix 2|Neoproterozoic|Mesoproterozoic|c.1300-c.850 Ma. Of Yeneena Supergroup. Underlain by Throssell Group. Geological Province: Yeneena Basin.||||||25-JUL-07
34421|Lamil Group|23594|5|Briefly described|p9 Fig. 6|Neoproterozoic|Mesoproterozoic|Overlying unit Tarcunyah Group. Underlying unit Throssell Group.||||||
34421|Lamil Group|23602|5|Briefly described|p7|||Of Yeneena Supergroup.||||||
34421|Lamil Group|23730|5|Briefly described|p5 Fig 2|Mesoproterozoic|Mesoproterozoic|Geological Province: Yeneena Basin.||||||
34421|Lamil Group|23742|5|Briefly described|p6||Mesoproterozoic|Of Yeneena Supergroup.||||||
34421|Lamil Group|23745|4|Described|p17|Neoproterozoic|Mesoproterozoic|See also page 7 Fig 5. Of Yeneena Supergroup. Geological Province: Yeneena Basin.||||||
34421|Lamil Group|23746|4|Described|p25|Neoproterozoic|Mesoproterozoic|Of Yeneena Supergroup.||||||
34421|Lamil Group|23758|4|Described|p5|Neoproterozoic|Neoproterozoic|Of Yeneena Supergroup. Geological Province: Yeneena Basin.||||||
34421|Lamil Group|23760|4|Described|p24|Neoproterozoic|Mesoproterozoic|Of Yeneena Supergroup. Geological Province: Yeneena Basin.||||||
34421|Lamil Group|23780|5|Briefly described|p181|Mesoproterozoic|Mesoproterozoic|||||||
34421|Lamil Group|23900|4|Described|p1537 Fig.2|Proterozoic|Proterozoic|Of the Yeneena Supergroup. Overlies the Throssell Group. Geological Province: Paterson orogen.||||||
34421|Lamil Group|24017|5|Briefly described|p9 Tb. 2|Neoproterozoic|Mesoproterozoic|||||||
34421|Lamil Group|24025|4|Described|p15|Neoproterozoic|Neoproterozoic|Of the Yeneena Supergroup.  Geological Province: Pilbara Craton.||||||
34421|Lamil Group|24110|5|Briefly described|Plate 1|Proterozoic|Proterozoic|Of the Yeneena Supergroup.  Geological Province: Yeneena Basin.||||||25-JUL-07
34421|Lamil Group|24194|4|Described|p898, p899 Fig.2, p900, Fig.3|Neoproterozoic|Neoproterozoic|Of the Yeneena Supergroup. Underlain by Throssell Group. Geological Province: Yeneena Basin.||||||25-JUL-07
34421|Lamil Group|24197|5|Briefly described|p100|||Formerly of the Yeneena Group. Occurs mainly in the Telfer area, containing the informally named "Telfer Succession". Geol. Prov: Paterson Orogen.||||||07-FEB-11
34421|Lamil Group|24496|6|Mentioned|p50|||Sediments.||||||21-DEC-04
34421|Lamil Group|24594|5|Briefly described|p602|Neoproterozoic|Mesoproterozoic|Age: ca1070-680Ma.  Unconformably overlies Rudall Complex.  Geological Province: Yeneena Basin (Paterson Orogen).  See also p601.||||||28-NOV-06
34421|Lamil Group|44111|6|Mentioned|p56 Fig.1, 60|||in Yeneena Basin, intruded by 620 Ma granitoids. Supersedes part of Yeneena Group. Deposited between 1790 and 1290 Ma. Underwent three episodes of deformation and greenschist facies metamorphism between 1290 and 820 Ma. Hosts important gold deposits (?related to 620 Ma granitoids) and base-metal mineralisation.||||||
34421|Lamil Group|49895|5|Briefly described|p2 Fig.1|Neoproterozoic|Neoproterozoic|Of the Yeneena Supergroup. Geological Province: Paterson Orogen.||||||
34421|Lamil Group|50008|5|Briefly described|p45 Fig.2|Neoproterozoic|Neoproterozoic|Geological Province: Yeneena Basin.||||||15-JUN-05
34421|Lamil Group|50188|6|Mentioned|p10 Fig. 3|||||||||
34421|Lamil Group|50228|5|Briefly described|p480 Fig.3|Mesoproterozoic|Mesoproterozoic|See also Lamil group. Sandstone-siltstone-shale-carbonate succession of rocks. Age: c. 1070Ma (zircons). Probably correlates with the Throssell Group.||||||28-NOV-06
34421|Lamil Group|50436|5|Briefly described|p1.1|||Of the Yeneena Supergroup. Intruded by O'Callaghans Supersuite.||||||30-JUL-04
34421|Lamil Group|50544|5|Briefly described|p11, p16 Tb. 1|Neoproterozoic|Neoproterozoic|Of the Yeneena Supergroup.  Age: c.1070-678Ma. (Bagas, 2000).  Geological Province: Yeneena Basin.||||||
34421|Lamil Group|50555|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Yeneena Supergroup - unassigned units on YARRIE. Geological Province: Yeneena Basin.||||||02-DEC-11
34421|Lamil Group|60470|4|Described|p1, 2-5, 7, 8, 9 , 10-11|Neoproterozoic|Neoproterozoic|in Yeneena Basin, of Yeneena Supergroup. Sandstone, siltstone, and carbonate rocks of Malu, Puntapunta, and Wilki Formations. 1070 Ma Max age from detrital zircons by Nelson (2000) and Bagas et al. (2002), 654 Ma min age from granite by Dunphy & McNaughton (1998). Hosts Telfer gold mineralisation.||||||11-JUN-13
34421|Lamil Group|62453|4|Described|p5 Fig. 3, 68|Cryogenian|Cryogenian|Geological Province: Paterson Orogen. Sandstone, shale, limestone and dolomite.||||||
34421|Lamil Group|62986|5|Briefly described|p18|Neoproterozoic|Neoproterozoic|Geological Province: Yeneena Basin. Also referred to as Lamil group.||||||
34421|Lamil Group|62987|6|Mentioned|p30|||In the Paterson Orogen.||||||
34421|Lamil Group|63417|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Geological Province: Yeneena Basin (Centralia Superbasin). Undivided, quartz sandstone, conglomerate, carbonate, siltstone, shale and pyritic shale.||||||20-AUG-07
34421|Lamil Group|64283|5|Briefly described|p50 Fig. 1, p54 Fig. 4|Neoproterozoic||Hosts the Telfer gold deposit.||||||07-FEB-11
34421|Lamil Group|64286|5|Briefly described|p76 Fig. 4|Neoproterozoic|Neoproterozoic|Age: <1000Ma.||||||07-FEB-11
34421|Lamil Group|64580|4|Described|map legend||Neoproterozoic|Quartz sandstone, conglomerate, carbonate, siltstone, and shale; minor pyritic shale.||||||15-DEC-08
34421|Lamil Group|64722|5|Briefly described|Fig. 2 p3-6, Fig 6 p15, p16, 22|Neoproterozoic|Neoproterozoic|Yeneena Basin? Sedimentary unit located in the Paterson region. This article considers this unit part of the Centralian Superbasin system, following Paleoproterozoic and Mesoproterozoic tectonic cycles represented by the Paterson Orogen.||||||
34421|Lamil Group|64724|5|Briefly described|p49 Fig. 7|Cryogenian|Cryogenian|Deposited in the Yeneena Basin during (and possibly continuing after) the Centralian 1 event (~840-824 Ma)||||||
34421|Lamil Group|64725|5|Briefly described|pp67-68. |Neoproterozoic|Neoproterozoic|Yeneena Basin. Separated from the Throssell Group by the Camel-Tabletop fault zone which extends southeast to the Musgrave Complex. Intruded by highly-fractionated I-type granites about 650 Ma.|||Includes Malu Formation.|||
34421|Lamil Group|64772|5|Briefly described|p14 Fig. 7, p35|||Telfer gold mineralisation and metalliferous iccurrences are associated with this unit.||||||07-FEB-11
34421|Lamil Group|64777|4|Described|p1-6, p8    |Neoproterozoic|Neoproterozoic|SHRIMP U-Pb detrital zircon populations at 1780 Ma, 1310-1000 Ma, and a minor group from 1670 to 1310 Ma. Most likely sources are northern Gascoyne Complex and NW Paterson Orogen.|||Includes the Wilki, Puntapunta and Malu Formations.||Consists of sandstone, siltstone and carbonate. No diagnostic stromatolitic or acritarch fossils have been found.|
34421|Lamil Group|64941|5|Briefly described|p27|Tonian|Tonian|Yeneena Basin.|||Malu Formation, Puntapunta Formation, Wilki Formation, Isdell Formation|Overlies Coolbro Sandstone (Throssell Range Group).|Sequence fining upwards.|
34421|Lamil Group|64943|4|Described|p1, 2, p3 Fig. 1, p13|Neoproterozoic|Neoproterozoic|Contact with Throssell (Range) Group not exposed, but interpreted to be a fault or unconformity from aeromagnetic data. Intruded by Mount Crofton Granite (age: c. 620 Ma)||||||
34421|Lamil Group|65366|6|Mentioned|p22 Fig.2|Neoproterozoic |Neoproterozoic |||||||
34421|Lamil Group|65403|5|Briefly described|p5, p13, p18.|||Intruded by several massive to weakly foliated (i.e. post-D4 Miles Orogeny event) granitoids.|> c.630 Ma.|Unit in Yeneena Supergroup.||Intruded by Mount Crofton Granite.||29-SEP-15
34421|Lamil Group|65454|5|Briefly described|p7-8, p12, p23|Cryogenian|Cryogenian|Of northeastern Yeneena Basin. Consists of Malu, Puntapunta and Wilki Formations. Intruded by O'Callaghans Supersuite||||||
34421|Lamil Group|65725|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|In diagrammatic section, overlain by Paterson Formation. Includes Malu, Puntapunta and Wilki Formations. Age <1070 Ma probably from Malu Formation. Province: Yeneena Basin (Centralian Superbasin)||||||26-FEB-13
34421|Lamil Group|65826|4|Described|p1, p5, p10, p12, pp13-14. |Neoproterozoic|Neoproterozoic|Yeneena Basin, Paterson Orogen. Intruded by post-orogenic I-type monzogranites and syenogranites aged c.654 Ma. Correlative of Throssell Range Group. The Miles Orogeny produced NW-trending folds and faults. Soft-sediment deformation is common, suggesting the Miles Orogeny was active during the early history of the Group.|c.820 - 654 Ma.||Includes Malu, Puntapunta and Wilki Formations.|||
34421|Lamil Group|67195|6|Mentioned|p6|||||||||
34421|Lamil Group|67202|4|Described|p50, p55, p57, p59-63, p118,p122 Fig.5.9|Neoproterozoic|Neoproterozoic|See also p128, p132, p141, p145, p156, p182-184, p189, p191, p195-196, p205, p237, p253. Yeneena Basin. Hosts the Telfer Au-Cu deposit. Gravity and aeromagmetic interpretation. Maximum and minimum ages are from detrital zircons and intrusion respectively. Conductivity image.|Between 950 Ma and 650 Ma.||Malu, Puntapunta, Wilki Formations.|Overlies Throssell Range Group. Is faulted against the Isdell Formation. Is intruded by the Mount Crofton Suite.|A sandstone-shale-carbonate succession, dominated by turbiditic sandstone interbedded with calcareous siltstone.|
34421|Lamil Group|68902|5|Briefly described|p5 fig 3, p6-7, p12, p17, p20|Neoproterozoic|Neoproterozoic|Regionally metamorphosed and repeatedly deformed, and intruded by c.650-630 Ma granite plutons. c.7 km thick. Extends to the basement of the Waukarlycarly Embayment.|||Includes Wilki Formation.|Probably overlies Throssell Range Group. Is overlain unconformably by the Paterson Formation.||18-JAN-17
34421|Lamil Group|68981|6|Mentioned|p3 Fig.2|||Paterson Orogen.||||||
34421|Lamil Group|69003|4|Described|p4, p23, p60-61, p64-65|Neoproterozoic|Neoproterozoic|Yeneena Basin, Paterson Orogen. Deformed by the c.650 Ma Miles Orogeny. Hosts significant Au-Cu mineralisation, particularly at the Telfer Dome, which may be related to intrusions of the O'Callaghans Supersuite.|||Malu, Puntapunta, Wilki Formations.|Is intruded by O'Callaghans Supersuite.|Includes interbedded siltstone and sandstone units.|
34421|Lamil Group|69167|6|Mentioned|geologyp_lut.csv|Neoproterozoic|Neoproterozoic||||Includes Malu Formation, Isdell Formation|||
34421|Lamil Group|69182|6|Mentioned|Ch4 p3|||Canning Basin. ||||||
34421|Lamil Group|69590|5|Briefly described|GEOL_LUT_CSV files|Neoproterozoic|Neoproterozoic|Geological province: Paterson Orogen. Events: Musgrave Orogeny; Paterson Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv2_5m_geologyp98_lut.|||Includes Malu Formation, Puntapunta Formation, Wilki Formation.|||
34421|Lamil Group|70826|6|Mentioned|p11|Neoproterozoic|Neoproterozoic|Rudall Province.Same age as the Centralian Superbasin.||||||
34421|Lamil Group|71080|6|Mentioned|p26|||Yeneena Basin. Probable Tonian age.|||Includes Malu Formation.|||
34421|Lamil Group|71169|6|Mentioned|p3 fig 2, p8, p16|Neoproterozoic|Neoproterozoic|Yeneena Basin.|c. 1070 Ma (Maximum depositional age)|||||
34421|Lamil Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||shale, siltstone|
34421|Lamil Group|71795|6|Mentioned|p34 fig 3|||Paterson Orogen.||||||
34421|Lamil Group|72034|5|Briefly described|500k_interpgeop16_lut|Ediacaran|Neoproterozoic|Yeneena Basin.|||Includes Wilki Formation, Puntapunta Formation, Malu Formation.||Quartz sandstone, conglomerate, carbonate, siltstone, and shale; minor pyritic shale.|
27459|Lamont Sandstone|14228|6|Mentioned|p9|Miocene|Miocene|Gascoyne Platform.||||||
27459|Lamont Sandstone|23311|5|Briefly described|map legend|Miocene|Miocene|||||||
27459|Lamont Sandstone|23403|4|Described|p9|Neogene|Paleogene|||||||07-NOV-08
27459|Lamont Sandstone|23569|6|Mentioned|p8|||||||||
27459|Lamont Sandstone|23620|5|Briefly described|p4 Fig. 4|Neogene|Neogene|Marine limestone and minor marine and continental sandstone||||||
27459|Lamont Sandstone|23726|5|Briefly described|p88|Middle Miocene|Oligocene|Overlying unit Trealla Limestone. Underlying unit Tulki Limestone. Geological Province: Carnarvon Basin.||||||
27459|Lamont Sandstone|23815|4|Described|p303|Middle Eocene|Middle Eocene|Geological Province: Carnarvon Basin. Underlying unit: Giralia Calcarentie (conformable). Overlying unit: Trealla Limestone (unconformable). Max. thickness: 10 m.||||||27-APR-05
27459|Lamont Sandstone|23976|5|Briefly described|Map Legend|Neogene|Neogene|||||||
27459|Lamont Sandstone|23977|5|Briefly described|Map Legend|Neogene|Neogene|||||||
27459|Lamont Sandstone|23978|5|Briefly described|Map Legend|Neogene|Neogene|||||||
27459|Lamont Sandstone|24351|5|Briefly described|Plate 4 (in pocket)|Middle Miocene|Early Miocene|Geological Province: Gascoyne Platform/Sub-basin.||||||13-DEC-07
27459|Lamont Sandstone|32750|6|Mentioned|p313|||Stratigraphic table||||||
27459|Lamont Sandstone|35105|6|Mentioned|Fig.5|||||||||
27459|Lamont Sandstone|36257|6|Mentioned|Table 2.1|||||||||
27459|Lamont Sandstone|36890|3|Fully described|p303|||||||||
27459|Lamont Sandstone|37016|6|Mentioned|Map legend|middle Miocene|middle Miocene|||||||
27459|Lamont Sandstone|37302|6|Mentioned|p75|||||||||
27459|Lamont Sandstone|38998|6|Mentioned|p25|||||||||
27459|Lamont Sandstone|39427|4|Described|Table 1|||||||||
27459|Lamont Sandstone|40340|6|Mentioned|p15|||||||||
27459|Lamont Sandstone|40342|6|Mentioned|Map legend|middle Miocene|middle Miocene|Prob.Middle Miocene||||||
27459|Lamont Sandstone|40343|5|Briefly described|p12|||||||||
27459|Lamont Sandstone|40617|6|Mentioned|p18|||||||||
27459|Lamont Sandstone|41271|3|Fully described|p184|||Mention P18. Of Cape Range Group.||||||
27459|Lamont Sandstone|42116|6|Mentioned|p69|||||||||
27459|Lamont Sandstone|44657|14|Not recorded|p.5,13,14|||||||||
27459|Lamont Sandstone|61155|5|Briefly described|p15|Middle Miocene|Middle Miocene|Of the Cape Range Group. Overlain by and interfingers with Pindilya Formation; partly overlain by Trealla Limestone. Age: 16-14Ma. Thickness: 3m.  Geological Province: Carnarvon Basin /onshore.||||||
27459|Lamont Sandstone|66125|6|Mentioned|p132|Miocene|Oligocene|Onshore Carnarvon Basin.||||||
27459|Lamont Sandstone|67200|5|Briefly described|p8 fig 6, |Miocene|Oligocene|||||Unconformably overlies Tulki Limestone, overlain by Trealla Limestone|Commonly massive pebbly sandstone.|
27459|Lamont Sandstone|69182|6|Mentioned|Ch3 p13|Miocene|Miocene|Gascoyne Platform, Carnarvon Basin. ||||||
27459|Lamont Sandstone|69558|5|Briefly described|p27, p98, p226|Miocene|Miocene|Exposed as rocky outcrops in some headlands on the east side of Hamelin Pool. Forms substrate for stromatolites. |||||Silicified sandstone.|
27459|Lamont Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
38642|Lancefield Conglomerate|23786|5|Briefly described|p5|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
38642|Lancefield Conglomerate|62106|5|Briefly described|p1365|Archean|Archean|Age: <2675+/-4 Ma (SHRIMP U-Pb). Geological Province: Laverton greenstone belt in Eastern Goldfields province of Yilgarn Craton.||||||07-NOV-08
38642|Lancefield Conglomerate|66880|6|Mentioned|p19. |Archean|Archean|Stratigraphically correlated with Wallaby Conglomerate.|2684 +/- 5 Ma.|||||
25151|Lancelin Formation|12758|5|Briefly described|p22, p3 Fig. 3|Cretaceous|Cretaceous|Of the Coolyena Group.||||||
25151|Lancelin Formation|12759|4|Described|p42; p28 Tb. 7; p32 Fig 15; P36 Fig 17|late Maastrichtian|Coniacian|Defined Lancelin Beds (Edgell, 1964); renamed in this study. Type section in Lancelin No.2B bore, (AMG Z50, 339929 m E, 6561788 m N) between 32-46 m depth, near Lancelin township, 100km N of Perth. Max thickness is 120 m.||Of Coolyena Group.||Conformably overles Gingin Chalk, and is unconformably overlain by Kings Park Formation.|White to greenish-brown, glauconitic marl.|12-MAY-14
25151|Lancelin Formation|14227|5|Briefly described|Enclos. 2|Late Cretaceous|Early Cretaceous|Of Coolyena Group. Presented as Lancelin Fm.||||||07-FEB-11
25151|Lancelin Formation|23279|6|Mentioned|p31|||||||||
25151|Lancelin Formation|41989|4|Described|p115|||||||||
25151|Lancelin Formation|43062|5|Briefly described|Table 2,p18|||Coolyena Group||||||
25151|Lancelin Formation|43347|6|Mentioned|9|||||||||
25151|Lancelin Formation|44144|4|Described|p503 Tb.4-21, p517|Maastrichtian|Santonian|Type Section: Lancelin 2B bore; 31o04'00''S 115o19'20''E; 32-46 (TD) m. 72m thick marine shelf deposits.||Coolyena Group||Passes laterally into Poison Hill Greensand, Gingin Chalk and Molecap Greensand.|White to green-grey glauconitic chalk, marly chalk, and dark-green calcareous mudstone.|
25151|Lancelin Formation|61811|4|Described|p3 Fig.2, pp54-57, p64.|Campanian|Coniacian|Northern Perth Basin. Known only from subsurface west of Gingin. Lateral equivalent of Poison Hill Greensand plus Gingin Chalk. Up to 120 m thick. Type section details in Appendix 1.||Unit in Coolyena Group.||Overlies Molecap Greensand.|Chalk.|
25151|Lancelin Formation|64580|4|Described|map legend||Late Cretaceous|Of Coolyena Group. Glauconitic chalk, marl, and calcareous mudstone.||||||09-DEC-08
25151|Lancelin Formation|64635|5|Briefly described|p4 Fig.3, |Maastrichtian|Coniacian|||Unit in Coolyena Group.||||
25151|Lancelin Formation|67115|6|Mentioned|p64 Fig. 2 |Cretaceous|Cretaceous|||||Overlies the Molecap Greensand.||
25151|Lancelin Formation|67340|6|Mentioned|p6|Late Cretaceous|Late Cretaceous|Northern Perth Basin.||Coolyena Group.||||
25151|Lancelin Formation|68254|6|Mentioned|p1036 Fig.2, p1046 Tb.4|Cretaceous|Cretaceous|||||||
25151|Lancelin Formation|68811|5|Briefly described|p92 fig 52, p180 tbl 39|Cretaceous|Cretaceous|||||Overlies the Kardinya Shale, Leederville Formation. Overlain by the Kings Park Formation.|Siltstone, shale and minor sandstone.|15-APR-20
25151|Lancelin Formation|69182|6|Mentioned|Ch2 p3, Ch2 p9|Upper Cretaceous|Upper Cretaceous|Perth Basin. See also Ch2 p45,Ch2 p55, Ch2 p57. ||Coolyena Group||Overlies the Molecap Greensand. Grades into the Poison Hill Greensand.||
25151|Lancelin Formation|70097|5|Briefly described|p19 Fig.3|Maastrichtian|Campanian|Perth Basin. Beermullah Trough.||Coolyena Group|||Limestone.|
25151|Lancelin Formation|72034|5|Briefly described|500k_interpgeop16_lut|Maastrichtian|Santonian|Perth Basin.  Age from biostratigraphy.||Coolyena Group|||Glauconitic chalk, marl, and calcareous mudstone.|
70736|Lancer Member|61023|6|Mentioned|p16|||Eolian sandstone facies. Geological Province: Officer Basin.||||||11-APR-08
70736|Lancer Member|62453|3|Fully described|p6 Fig. 4, 19, 27|Cryogenian|Cryogenian|Of the Browne Formation. Correlates with Mundadjini Formation and Skates Hills Formation. Sandstone. Overlies: Browne Formation. Underlies: Hussar Formation.||||||
70736|Lancer Member|63022|5|Briefly described|p1016 Fig. 2|Neoproterozoic|Neoproterozoic|Of the Browne Formation. Geological Province: Officer Basin. Reddish brown cross-bedded sandstone in foresets up to 11 m thick.||||||10-AUG-07
70736|Lancer Member|65363|2|Defined|p1, p6 Fig.5, p10, pp37-38.|Neoproterozoic|Neoproterozoic|New name. Type section is the interval 1201.9 to 1297.7 m in Lancer 1. Eolian dune deposit; siltstone intercalated beds are presumably interdune deposits in ephemeral lakes. Correlates with halite-dominated evaporites in other drillholes in the Officer Basin. May correlate with sandy facies in the upper part of Mundadjini Formation which has similar large cross-bedding. Excellent reservoir quality.||Topmost unit in Browne Formation.||Is overlain by Hussar Formation, probably disconformably.|Eolian sandstone: orange-brown, generally medium-grained, very well-sorted, well-rounded and porous, cross-bedded quartz sandstone in foresets up to 11 m thick; minor silty beds to 0.6 m thick.|
70736|Lancer Member|65364|5|Briefly described|p81|||Officer Basin.||Top of Browne Formation.|||Redddish-brown cross-bedded sandstone in foresets up to 11 m thick.|16-MAR-12
70736|Lancer Member|65365|5|Briefly described|p8 Fig.3|||Of Browne Formation, Buldya Group.||||||19-MAR-12
70736|Lancer Member|65371|5|Briefly described|p54 Fig. 1|||Of Browne Formation. Cross bedded sandstone, foresets up to 11m thick. Eolian depositional environment||||||
70736|Lancer Member|67454|5|Briefly described|p563 Fig.2, p564.|Neoproterozoic|Neoproterozoic|Officer Basin.||Unit in Browne Formation.|||Dominantly sandstone.|
69780|Lander Rock Formation|61405|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group. Includes the Yinabalbu Member and three unnamed facies: greenschist, amphibolite and granulite facies.  Age: >1835Ma.  Geological Province: Arunta region - Aileron Province.||||||07-NOV-08
69780|Lander Rock Formation|62632|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Tanami/Arunta Region-Aileron Province. Greenschist facies schist, amphibolite facies schist, granulite facies, gneiss.||||||07-NOV-08
69780|Lander Rock Formation|62633|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region - Aileron Province. Greenschist facies metapsammite and metapelite, schist. Amphibolite and Granulite facies schist and gneiss.||||||07-NOV-08
69780|Lander Rock Formation|62636|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region - Aileron Province.|||Includes Yinabalbu member.||Greenschist, amphibolite and granulite facies; gneiss, schist.|19-DEC-12
69780|Lander Rock Formation|62637|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Tanami/Arunta Region - Aileron Province. Greenschist and amphibolite facies schist, psammite and greywacke.||||||23-DEC-09
69780|Lander Rock Formation|62642|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Undifferentiated mica, hornblende biotite and amphibolite, dolerite; schist. Geological Province: Arunta Region - Aileron Province.||||||07-NOV-08
69780|Lander Rock Formation|63866|5|Briefly described|p93|||Reynolds Range, Aileron Province.|c. 1790 Ma|||||
69780|Lander Rock Formation|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Interbedded psammite and pelite; quartz-muscovite schist; may include meta-banded iron-formation and Interbedded metabasalt, metarhyolite and metavolcaniclastic rocks, including metavolcanic conglomerate.||||||15-DEC-08
69780|Lander Rock Formation|64677|5|Briefly described|v, p1, p24-26, p55-56|||Arunta Region, Aileron Province. Complex range of ages discussed: an alternative maximum depositional age is 1773 +/- 12 Ma.|1842 +/- 7 Ma (maximum depositional age).||||Metapsammite, quartz-muscovite-biotite schist, migmatite.|
69780|Lander Rock Formation|64735|6|Mentioned|p215, p217|||Similar detrital zircon age spectra to Bullion Schist; correlated with Mount Stafford Beds of Vernon et al (1990).||||||
69780|Lander Rock Formation|64736|4|Described|p220, 221-2, p224-225, p227, Figs.1, 8|Orosirian|Orosirian|Thickness unknown. SHRIMP U-Pb detrital zircon max depositional age.|1868 Ma.|Of Lander Package.||Underlies Reynolds Range Group unconformably.|Dominantly consists of interbedded pelitic and psammitic metasediments, interpreted to represent turbiditic sedimentation. Interlayered igneous rocks.|30-APR-12
69780|Lander Rock Formation|64737|4|Described|p231, 235, 236-42, 244,Tab.1, Figs.5, 6||Orosirian|Formerly known as Lander Rock Beds.  Name used for low grade metamorphic rocks in the Aileron Province. Occupies more than 60% of exposure in the Aileron Province. Thickness unknown. Intruded by Stafford Event plutons. Provenance dominated by ~1880-1840 ages||Of Lander Package.|||Interbedded pelitic and psammitic rocks interpreted to represent dominantly turbiditic sedimentation. Locally interlayered basalt and dolerite.|30-APR-12
69780|Lander Rock Formation|65329|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Shown as older than Reynolds Range Group, Ngadarunga Granite.  Greenschist facies; schist, quartzite; Amphibolite facies: biotite-muscovite schist,  quartz granofels; Granulite facies: migmatitic gneiss, quartzite, mafic gneiss||||||
69780|Lander Rock Formation|65330|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Shown as older than Reynolds Range Group, Ngadarunga Granite.  Greenschist facies; schist, quartzite; Amphibolite facies: biotite-muscovite schist,  quartz granofels; Granulite facies: migmatitic gneiss, quartzite, mafic gneiss;  ||||||
69780|Lander Rock Formation|65332|5|Briefly described|Map Legend|Palaeoproterozoic|Palaeoproterozoic|Informally subdivided into four facies with with distinctive magnetic responses. Greenschist-facies interbedded metapsammite and metapelite; amphibolite-facies schists, metapsammite; granulite-facies migmatitic gneiss; retrogressed gneiss ||||||
69780|Lander Rock Formation|65333|5|Briefly described|Map Legend|Orosirian|Orosirian|In some places differentiated into Walabanba and Anningle members, and two unnamed members. Succession of metasedimentary and stratiform mafic (meta-)igneous rocks.||||||
69780|Lander Rock Formation|65334|5|Briefly described|Map Legend|Orosirian|Orosirian|In some places differentiated into Walabanba and Anningle Members, and two unnamed members. Succession of metasedimentary and stratiform mafic (meta-) igneous rocks.||||||
69780|Lander Rock Formation|65335|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Aileron Province. Includes Yinabalbu member. Age: older than Stafford Event (1805 Ma)?. Dominantly quartz-muscovite-biotite pelitic schist and phyllite interlayered with quartz-muscovite psammite; includes a component of high-grade metasediments||||||
69780|Lander Rock Formation|65338|3|Fully described|App1 p82, p6-17|Statherian|Orosirian|Shallow to deep-water marine. Definition only gives maximum depositional age from detrital zircons. Minimum age from intrusion by Harverson Granite at 1799+/-3Ma. Correlated with Ooradidgee Group, at least in part. Greenschist to granulite facies metamorphism from c.1805-1790 Stafford Event with syn-tectonic granite intrusions. Hosts orogenic gold. Monotonously uniform and widespread.|c.1840 - 1799 Ma.||Includes Walabanba, Anningie, Woodalla and Mount Stafford Members.|Intruded by Koonoonyeri granites, Yaningidjara Orthogneiss, Harverson Granite, dolerite and gabbro. Is overlain by Reynolds Range Group.|Metapsammitic and metapelitic rocks: hornfels, slate, phyllite and schist, variably metamorphosed from greenschist to granulite grade; stratiform amphibolites; rare calc-silicate rocks.|
69780|Lander Rock Formation|65341|6|Mentioned|p2 Fig.2. |Paleoproterozoic|Paleoproterozoic|||||Grouped with Reynolds Range Group in Fig 2.||19-DEC-12
69780|Lander Rock Formation|65343|5|Briefly described|p3 Fig.4|Paleoproterozoic|Paleoproterozoic|Arunta Region. See also Lander Rock beds.||||||
69780|Lander Rock Formation|65358|5|Briefly described|p6, p10-11, p13, p17-18|Orosirian|Orosirian|In Arunta Region. Unconformably overlain by Reynolds Range Group. Correlated with Killi Killi Formation in Tanami Region. Turbiditic. Deposited at ~1860-1830 Ma; metamorphosed to greenschist to granulite facies.||||||
69780|Lander Rock Formation|65556|5|Briefly described|p29, p37, p44-45||Orosirian|Sedimentary rocks. Widespread in the Arunta Region. Similar age spectra to rocks analysed in this study suggest correlation with the Casey Inlier and Anira Metamorphics. ~1830 Ma maximum depositional age. Intruded by Stafford Event magmatic intrusions at ~1810-1800 Ma.||||||
69780|Lander Rock Formation|66767|6|Mentioned|p57|||Aileron Province.||||||
69780|Lander Rock Formation|67163|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.|||||Quartz muscovite-biotite schist, fine- to medium-grained, layered; granulite-facies pelitic, migmatitic gneiss; granulite, strongly foliated and folded; metapsammite.|
69780|Lander Rock Formation|67164|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province. Several separately-mapped but un-named units have their lithologies and magnetic responses indicated.|||Includes Anningie, Walabanba, Woodalla and Mount Stafford Members.||Undifferentiated mica, hornblende-biotite and hornblende schist; phyllite; heavy mineral-bearing/micaceous quartzite; amphibolite; dolerite; rare muscovite-sillimanite, and microcline-sillimanite-garnet-bearing schist.|
69780|Lander Rock Formation|67165|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province. Parts of this unit are mapped according to the strength of their magnetic responses.|||||Dominantly greenschist facies: quartz-muscovite psammite, micaceous greywacke, quartz-muscovite schist; includes amphibolite facies: micas-andalusite schist and psammite; lesser granulite facies: migmatite with psammitic layers.|
69780|Lander Rock Formation|67352|6|Mentioned|p50|||||||||
69780|Lander Rock Formation|67479|6|Mentioned|p56|||Comprises a widespread body of typically low-grade metasedimentary rocks.||||||
69780|Lander Rock Formation|67892|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.|||Includes Mount Stafford, Woodalla, Anningie and Walabanba Members.||Undifferentiated: mica, hornblende-biotite and hornblende schist; phyllite; heavy mineral-bearing/micaceous quartzite; amphibolite, dolerite; rare muscovite-sillimanite, and microcline-sillimanite-garnet-bearing schist.|
69780|Lander Rock Formation|68656|5|Briefly described|GEOCHRON|Paleoproterozoic|Paleoproterozoic|Arunta Orogen. Widespread unit. Age is maximum depositional age from detrital zircons.|1838 +/- 15 Ma (Kirkland et al., 2009).|||Is correlated with Killi Killi Formation.||
69780|Lander Rock Formation|68697|6|Mentioned|v, p44|||N, W and Central Aileron Province. Typical detrital zircon spectrum is dominated by post-1900 Ma ages.||||||18-APR-18
69780|Lander Rock Formation|68994|4|Described|p4, p6-12, p20, p23-24, p26-27|Orosirian|Orosirian|Widely distributed, though poorly exposed over northern and western Aileron Province. Metasandstone analysed. Conservative max depositional age of 1872+/-5 Ma (Kirkland et al. 2009). Detrital zircon U-Pb ages listed and Hf analyes detailed.|1840-1830 Ma (Scrimgeour 2006).|||Intruded by Carrington Suite granitic rocks. Equivalent to Killi Killi Formation (Tanami Group). Is unconformably overlain by Munyu Sandstone.|Polydeformed, psammitic and pelitic schists (interbedded quartz-muscovite-biotite schist) and minor interbedded banded-iron formation; predominantly greenschist to amphibolite facies; interpreted largely turbiditic origin.|13-JAN-17
69780|Lander Rock Formation|68997|4|Described|vi-vii,p1,26-28|Orosirian|Orosirian|Widely distributed unit that is sporadically exposed across much of the northern and western Aileron Province. Oldest exposed rocks in the Aileron Province. Similar stratigraphic position to Aileron and Chiripee Metamorphics. Oldest zircon spectra includes c. 3438 Ma. Zircon age spectra from psammitic gneiss (Sample: AC08CJE271A. Grid Reference: MGA94 Zone 53: 370504mE 7550491mN) of 1835+\-6 Ma (in northwestern ALCOOTA), interpreted as maximum depositional age. Metamorphic zircon rims dated at 1763+\-6 Ma are interpreted to reflect a marginally younger event than the 1780-1770 Ma Yambah Event.|1835+\-6 Ma (max dep age: U-Pb zircon)||||Interbedded pelitic and psammitic metasedimentary rocks; turbiditic.|
69780|Lander Rock Formation|68998|5|Briefly described|v, p12-13, p31|Paleoproterozoic|Paleoproterozoic|||||Is intruded by Ennugan Mountains Granite.||
69780|Lander Rock Formation|69003|5|Briefly described|p5, p31|Paleoproterozoic|Paleoproterozoic|Aileron Province, West Arunta Orogen.|1840-1835 Ma.|||Is intruded by the Carrington Suite.|Polydeformed metasedimentary rocks.|
69780|Lander Rock Formation|69031|5|Briefly described|p3-4, p6-7, p12, p23, p43, p50, p59, p79|Orosirian|Orosirian|Oldest outcropping rocks in the Aileron Province, Arunta Orogen. Detrital zircon age spectra described. Quartz veins and pegmatite host base metal deposits (eg Clark and Mount Hardy Cu prospects). Has a distinct magnetic response (discussed). Uranium-enriched: distance to this unit was used as a predictor in modelling for U sources.|1840-1835 Ma.|||Is intruded by Carrington Suite.|Polydeformed psammitic and pelitic rocks, and minor interbedded BIF.|
69780|Lander Rock Formation|69288|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region. Most outcrops are weathered to saprock: original textures and fabrics are preserved, but mineralogy has been predominantly replaced. Three facies are mapped separately: greenschist facies, amphibolite facies, and transitional amphibolite-granulite to granulite facies.|||||Quartz-muscovite+biotite schist; quartz-muscovite+biotite+andalusite+garnet+tourmaline schist; pelitic, psammopelitic and lesser psammitic migmatitic gneiss, lesser felsic migmatitic gneiss, minor mafic granulite.|
69780|Lander Rock Formation|69383|6|Mentioned|p70, 72, 74, 80|||Arunta Region. Includes inherited zircon population in the 1880-1800 Ma range, as does Utopia Quartzite.||||||
69780|Lander Rock Formation|69417|5|Briefly described|p2:4,|Orosirian|Orosirian|Aileron Province. Turbiditic succession.|1845-1835 Ma.|||||12-JUL-16
69780|Lander Rock Formation|69418|6|Mentioned|p3:21, 31, 33|||Arunta Region. Hosts the Anningie field pegmatite Sn deposit and the Mount Doreen field (Wolfram Hill) pegmatite W deposit (described). Also hosts the Nolans Bore phosphate-REE-U deposit (described).||||||12-JUL-16
69780|Lander Rock Formation|69424|5|Briefly described|p9:4, 34|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Region. Experienced bimodal magmatism and folding during the c.1800 Ma Stafford Event.||||Correlative of Ooradidgee Group.||12-JUL-16
69780|Lander Rock Formation|69425|6|Mentioned|p10:6||||||||Includes schists.|12-JUL-16
69780|Lander Rock Formation|69426|5|Briefly described|p11:4 Fig.11.3, 11:11|||Occurs extensively over N and W Aileron Province. The two facies associations are mapped separately in Fig.11.3.||||Correlated with Killi Killi Formation.|Amphibolite-facies pelitic and psammitic schist, gneiss; granite. Greenschist- to amphibolite-facies pelitic and psammitic schist, gneiss; granite.|12-JUL-16
69780|Lander Rock Formation|69427|3|Fully described|p12:3-7,13,18-22,24-27,29,32-33,41|||See also 12:57,59-60,62. Donnellan (2008). Formerly Lander Rock beds of Stewart et al. (1980), Stewart (1981), Young et al. (1995). Widely distributed across N and W Aileron Province. Interbedded pelitic and psammitic rocks of predominantly turbiditic origin. Crops out poorly. Type locality at Lander Rock. Neither base nor top is exposed; suggested minimum thickness 1000m. Equivalent of Killi Killi Formation and Ooradidgee Group. Metamorphic grade varies from greenschist to granulite facies, mapped separately. Deformation described in some detail. Mafic intrusions described. Some areas of this unit mapped by Stewart (1981) were included by Dirks (1990) in his version of the Reynolds Range Group. Detrital zircon maximum depositional age; other ages given. Likely that deposition was between 1840-1830 Ma. Metamorphic zircon rims are dated at 1806 +/- 7 Ma (Kinny, 2002) and c.1760 Ma (Claoue-Long and Scrimgeour, unpublished). Hosts a number of lode gold occurrences (briefly described). Associated with the Nolans Bore REE-P-U-Th deposit (detailed).|<1858 +/- 4 Ma (Claoue-Long et al., 2008).||Mount Stafford Member.|Is overlain by Mount Thomas Quartzite. Is intruded by Stafford, Ooralingie, Redhackle, Wabudali and Bean Tree Granites; Boothby Orthogneiss, Napperby Gneiss and Yumurrpa Granophyre.|Monotonous succesion of lineated biotite-muscovite-andalusite schist, micaceous metasandstone and quartzite; cleaved siltstone and slate; migmatitic units; local minor calc-silicate rock, conformable mafic layers (mainly amphibolite).|12-JUL-16
69780|Lander Rock Formation|69440|5|Briefly described|p25:2|||||||Is overlain unconformably by Munyu Sandstone.|Metasediments including intensely weathered, strongly foliated quartz-mica-feldspar schist.|12-JUL-16
69780|Lander Rock Formation|69508|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province. Four un-named subunits are mapped separately.|||||Granulite-facies sillimanite-garnet-biotite-cordierite migmatite with small mafic granulite inclusions, rare quartzite. Amphibolite-facies quartz-muscovite-biotite(-andalusite) schist, interbedded metapsammite and metapelite, quartz-muscovite schist.|
69780|Lander Rock Formation|69554|6|Mentioned|p139|||Aileron Province, Arunta Region, Northern Australian Craton. Contains detrital zircons aged c.1920 Ma.||||||
69780|Lander Rock Formation|69587|5|Briefly described|177278.1.pdf|||Geological province: Arunta Orogen. Kirkland et al. (2009) reported a maximum depositional age of 1838+\-15 Ma for a metasandstone sample.|c. 1840-1830 Ma|||Correlable with Killi Killi Formation.||
69780|Lander Rock Formation|69794|6|Mentioned|p16|||Comprises c. 1865 Ma zircon provenance peak, with broad clusters between 2000-1900 Ma and 2550-2500 Ma, and sporadic Archean ages.||||||
69780|Lander Rock Formation|69917|4|Described|p55-57, 117, 82, 87, 93||Paleoproterozoic|Central Arunta Region, Aileron Province. U/Pb SHRIMP zircon dating, Hf analytical data. Dating indicates maximum depositional age of 1835+/-6 Ma and metamorphic zircon growth during the high-grade 1780-1770 Ma Yambah Event||||Intruded by Woola Downs Granite. Detrital zircon signature similar to Delny Metamorphics.|Psammitic gneiss.|
69780|Lander Rock Formation|70301|5|Briefly described|p7, p11, p16, p19|Paleoproterozoic|Paleoproterozoic|Mentioned as having ages typical of 2394-1974 Ma zircons occurring in Wangala Granite.||||Is intruded by Wangala Granite and Ennugan Mountains Granite.|Metasedimentary rocks.|
69780|Lander Rock Formation|70376|5|Briefly described|p832, p832 fig 1, p847|Paleoproterozoic|Paleoproterozoic|Intruded by magmatic rocks in the 1810 - 1770 Ma period. Shown as Lander Package p849.|1866-1806 Ma|||Unconformably overlain by Reynolds Range Group|Greywacke, siltstone, shale, schist, gneiss, pelites and psammitic metasediments.|
69780|Lander Rock Formation|70554|4|Described|p798,815|Paleoproterozoic|Paleoproterozoic|Geologial province: Aileron province. Comprised of two similar but temporally discrete (1840-1810 and 1805-1780 Ma) turbiditic packages. Underwent high-grade (to granulite-facies) metamorphism during Chewnings Orogeny and emplacement of late-metamorphic pegmatites (Collins and Williams, 1995).|||||Psammitic metasedimentary rocks; schist, phyllite, andalusite hornfels, garnet-cordierite-biotite-quartz granofels, sillimanite-biotite-cordierite-orthoclase granofels and tourmaline-bearing quartzite.|
69780|Lander Rock Formation|70739|6|Mentioned|p540|||Arunta Region. Has correlatives in the Tanami and Tennant Creek Regions.|1860-1830 Ma.|||||
69780|Lander Rock Formation|70762|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Orogen, North Australian Craton. Two un-named sub-units are mapped separately: metamorphosed BIF interbedded with psammitic and pelitic schist; and felsic volcanic metasandstone and metaconglomerate interbedded with amygdaloidal metabasalt.|<1840 Ma.|||Is overlain by Lake MacKay Quartzite.|Interbedded psammitic and pelitic schist; quartz-muscovite schist; may include metamorphosed BIF and metavolcanic rocks.|
69780|Lander Rock Formation|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|Aileron Province.||||||
69780|Lander Rock Formation|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region. In the Interpreted Geology diagram, this unit is mapped as two facies, each including undivided granite of Grimwade and Frederick Suites: amphibolite facies pelitic and psammitic schist, gneiss; and greenschist to amphibolite facies pelitic and psammitic schist, gneiss.|||||Biotite-muscovite-andalusite +/- garnet pelitic schist and metapsammite.|
69780|Lander Rock Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||pelite, gneiss, greywacke, amphibolite, psammite, schist|
69780|Lander Rock Formation|71302|5|Briefly described|p73|Paleoproterozoic|Paleoproterozoic|Geological province: Arunta region. Paleoproterozoic metasedimentary sequence exposed on the North Australian Craton, and possibly one of several sources of zircon provenance to the Inverway Metamorphics.||||||
69780|Lander Rock Formation|71348|5|Briefly described|p198,201,209,211-212,214-218|Orosirian|Orosirian|Geological province: Aileron Province, Arunta Region. Maximum depositional age between c. 1860 Ma and c. 1830 Ma. Also contains c. 2100-1900 Ma zircon, and Neoarchean to earliest Paleoproterozoic detrital zircon component. Underwent HTLP metamorphism, moderate strain and intrusion by felsic and mafic intrusions from c. 1780-1770 Ma Yambah Event. See p215 for summary of U-Pb geochronological data.||||Overlain unconformably by Reynolds Range Group and Lake Mackay Quartzite.||
69780|Lander Rock Formation|71810|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Orogen, North Australian Craton.|<1838 Ma.||||Interbedded psammitic and pelitic schist, quartz-muscovite schist; may include metamorphosed BIF and metavolcanic rocks.|
69780|Lander Rock Formation|71839|5|Briefly described|iii, p7-p8|||Hosts mineralisation at the Silver King Cu-Pb-Zn-Ag prospect in central DOREEN. U-Pb SHRIMP maximum depositional zircon ages range from 1869+/-4 to 1858+/-4 Ma.|||||Muscovite-sericite schist.|21-MAR-23
69780|Lander Rock Formation|71858|4|Described|p5-p6, p44-p45|||Aileron Province.|ca 1860-1830 Ma||Includes the Mount Stafford beds and the Walabanba Member.|Unconformably overlain by the Wickstead Creek beds (Reynolds Range Group). Intruded by the Wangala Granite and the Ennugan Mountains Granite.||
69780|Lander Rock Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Orogen.|||||Interbedded psammite and pelite; quartz--muscovite schist; may include metamorphosed banded iron-formation and metavolcanic rocks.|
69780|Lander Rock Formation|72366|4|Described|p1-2,4-5, p7|Orosirian|Orosirian|Geological province: Aileron Province. Hosts the Mount Hardy Cu-Pb-Ag-Zn deposit (MOUNT DOREEN map sheet). Intruded by barren and mineralised pegmatites, and mineralised quartz veins (Kiek 1941, Grainger 1968, Scrimgeour 2013). Maximum depositional age provided from SHRIMP U-Pb dating ranging between c. 1869 to 1858 Ma and peak zircon spectra at c. 1880-1840 Ma (Donnellan 2008, Scrimgeour 2013 and references therein). Sample MD15MVM001 (766491mE 7552939mN; molybdenite) is from molybdenite-bearing quartz vein in pegmatite selvage that intrudes into quartz-muscovite schist of the LRF; yields Re-Os model age of 1799.9+\-7.8 Ma (consistent with Ngadarunga Granite). Sample MD16MVM078 (766405mE 7552941mN, molybdenite) is from a quartz-muscovite pegmatite intruding in LRF; yields Re-Os model age of 1817.4+\-8.7 Ma. These ages are interpreted to represent magmatic crystallisation ages and the timing of pegmatite emplacement. Preserves zones of partial melting around contact zones with Ngadarunga Granite.||||Correlable to Killi Killi Formation. Intruded by Ngadarunga Granite.|Interbedded turbidites: pelitic and psammitic metasedimentary rocks.|08-JAN-20
69780|Lander Rock Formation|72376|5|Briefly described|iii,p1,3,6|Paleoproterozoic|Paleoproterozoic|Geological province: Aileron Province. Hosts the Wilfram Hill tungsten-copper deposit, which is intimately associated with muscovite-bearing pegmatite and quartz veins that intrude and cross-cut the Lander Rock Formation. Mineralisation is hosted in two main reefs of pegmatite and quartz veins (Wells 1972, Warren et al 1974, Young et al 1995). Previous studies provide U-Pb SHRIMP maximum depositional zircon ages spanning from 1869+\-4 Ma to 1835+\-6 Ma (Claoue- Long et al 2008, Donnellan 2008, Scrimgeour 2013, Bodorkos et al 2013). 40Ar/39Ar analysis of sample NTGS MD15MVM015 (muscovite in muscovite-bearing pegmatite that intrudes foliated muscovite schist of Lander Rock Formation) yielded an interpreted minimum age of 1550+\-4 Ma for tungsten and copper mineralisation at Wolfram Hill deposit; this age is consistent with that of Yarunganyi Grantie (1567+\-11 Ma; Young et al., 1995).|||||Foliated, metasedimentary, lower amphibolite facies biotite-muscovite-andalusite-quartz schist and minor metasandstone.|
69780|Lander Rock Formation|72378|5|Briefly described|p22|Paleoproterozoic|Paleoproterozoic|Geological province: Aileron Province. Regionally widespread unit, with a maximum depositional age of c 1.86-1.84 Ga (Claoue-Long et al., 2008a; Bodorkos et al., 2013; Scrimgeour 2013) and a likely depositional age of c. 1.84 Ga (Cross and Crispe 2007).||||Correlable with Bullion Schist.||
69780|Lander Rock Formation|72516|6|Mentioned|p7|||Aileron Province.||||||
69780|Lander Rock Formation|72527|6|Mentioned|p184, p192.|Paleoproterozoic|Paleoproterozoic|Given as an example of correlated units across the Northern Territory with the Murphy Metamorphics. Ref Hollis et al., 2010; Carson, 2013; Cross and Crispe, 2007; Bodorkos et al., 2013; Kositcin et al., 2012, 2013, 2014, 2015a).||||||
69780|Lander Rock Formation|72711|6|Mentioned|p4 Tb.1, p5-6, p6 Fig.4.|Orosirian|Orosirian|Maximum depositional ages of 1840-1830 Ma. (detrital zircon 207Pb/206Pb ages; Young et al 1995, Pietsch 2001, Claoue-Long and Edgoose 2008, Donnellan 2008). These are the oldest known rock formations in the Aileron Province.|c. 1840 Ma. to c. 1830 Ma max. dep.ages||||Includes metasedimentary gneiss and schist, metamudstone, lenses of massive breccia.|
69780|Lander Rock Formation|72894|5|Briefly described|piii, p1, p5-8, p10-13, p16, p19, p23|Statherian|Orosirian|Geological Province: Aileron Province; listed geochronology represents conservative maximum depositional ages for the sedimentary protolith from two samples; high-grade metamorphism is dated at 1769 +/- 14 Ma and 1761 +/- 4 Ma from two samples; unnamed samples of mafic granulite, metapsammite, and S-type granite were dated and correlated to the Lander Rock Formation|1832 +/- 10 Ma and 1841 +/- 8 Ma SHRIMP U-Pb||||Granulite-facies metasedimentary rocks; metapelites that locally have garnet-bearing leucosome patches interlayered with cordierite-biotite-garnet-quartz metapsammite; intermingled with coarse-grained S-type granite (formed from in-situ from melting)|
69780|Lander Rock Formation|73083|6|Mentioned|p11|Orosirian|Orosirian|An age of deposition of 1840-1830 Ma was reported by Scrimgeour (2013). Not equivalent to Ledan Schist.|1840-1830 Ma|||Equivalent to Ooradidgee Group.||
69780|Lander Rock Formation|73089|6|Mentioned|p3, p32-33, p41|Paleoproterozoic|Paleoproterozoic|Aileron Province. Dominantly Paleoproterozoic detritus. Has a similar lithology and provenance signature to both the Killi Killi and Olympio formations. Deposited sometime between c. 1872-1835 and 1820-1770 Ma.||||||
69780|Lander Rock Formation|73399|6|Mentioned|p2, App.E|Orosirian|Orosirian|Oldest rocks in the Reynolds-Anmatjira Ranges. Metamorphosed by voluminous granitic magmatism between 1810 and 1790 Ma. [Previously called the Lander Rock Beds].|ca. 1840 to 1806 Ma|||Unconformably overlain by the Reynolds Range Group.|Pelitic and psammitic metasedimentary rocks.|
69780|Lander Rock Formation|73445|5|Briefly described|p7|||West Arunta Orogen. Is intruded by 1773 +/- 6 Ma granitic rocks.|1840-1835 Ma (MDA: Scrimgeour, 2006).|||Is overlain by Lake McKay Quartzite.|Metasedimentary rocks.|
69780|Lander Rock Formation|73592|5|Briefly described|p3, 9-10|Paleoproterozoic|Paleoproterozoic|Aileron Province. Several other maximum depositional age determinations are given. Intruded by c.1820-1770 Ma granites. Deformed at c.1810-1790 Ma.|1855 +/- 4 Ma (MDA: Kositcin et al., 2019).|||Likely correlative of Bullion Schist.|Sedimentary, volcanic and volcaniclastic rocks.|
69780|Lander Rock Formation|74204|5|Briefly described|p2|Orosirian|Orosirian|Tightly folded during the Stafford Event (1810-1800 Ma).|1840-1810 Ma||||Thick package of turbidite-related mudstones and sandstones.|
31958|Landor Granite|24197|6|Mentioned|p71 Tb. 7.1|||Of the Minnie Creek Supersuite.||||||07-FEB-11
31958|Landor Granite|50425|5|Briefly described|p1.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Province. Of the Minnie Creek Supersuite.||||||07-NOV-08
27180|Landrigan Tillite|22496|5|Briefly described|p11|Neoproterozoic|Neoproterozoic|Of the Kuniandi Group.  Correlates with the Moonlight Valley Tillite.||||||16-AUG-04
27180|Landrigan Tillite|22764|4|Described|Table1,p6||Adelaidean|Of the Kuniandi Group. Thickness:  210 m. Unconformable on Olympio Formation; inferred to be conformable beneath Bulka Hills Beds.||||||01-FEB-10
27180|Landrigan Tillite|23314|6|Mentioned|334|||||||||
27180|Landrigan Tillite|23621|5|Briefly described|p33|||Of Kuniandi Group.||||||
27180|Landrigan Tillite|23806|6|Mentioned|p1121|Neoproterozoic|Neoproterozoic|Of Kuniandi Group.See also Landrigan tillite.||||||
27180|Landrigan Tillite|24173|5|Briefly described|p25|Neoproterozoic|Neoproterozoic|Of the Kuniandi Group. Correlates with Moonlight Valley Tillite.||||||06-APR-05
27180|Landrigan Tillite|30533|6|Mentioned|p21|||Correlated with Mount House Group||||||
27180|Landrigan Tillite|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
27180|Landrigan Tillite|32660|5|Briefly described|Table 6|||||||||
27180|Landrigan Tillite|32728|6|Mentioned|Table 7|||See also Fig.16||||||
27180|Landrigan Tillite|35120|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
27180|Landrigan Tillite|36048|6|Mentioned|p379|||||||||
27180|Landrigan Tillite|36551|6|Mentioned|Table 10|||||||||
27180|Landrigan Tillite|36888|4|Described|p215|||||||||
27180|Landrigan Tillite|36898|6|Mentioned|p181|||||||||
27180|Landrigan Tillite|37462|5|Briefly described|p294|||||||||
27180|Landrigan Tillite|37927|4|Described|p504|||||||||
27180|Landrigan Tillite|38157|6|Mentioned|Table X|||||||||
27180|Landrigan Tillite|41405|5|Briefly described|p206|||||||||
27180|Landrigan Tillite|42661|6|Mentioned|p120|||||||||
27180|Landrigan Tillite|42811|5|Briefly described|p30|||||||||
27180|Landrigan Tillite|43666|6|Mentioned|p51,Table 2||Neoproterozoic|||||||
27180|Landrigan Tillite|44140|5|Briefly described|p301 Fig.4-7, p303 Tb.4-2.|Neoproterozoic|Neoproterozoic|Of Mount Ramsay area. 17-335m thick. Mis-spelt as Landrigen Tillite in Fig.4-7.||Kuniandi Group||Overlain by Stein Formation conformably.|Tillite, lenses of sandstone and siltstone. Capped by dolomite.|07-MAR-18
27180|Landrigan Tillite|44231|5|Briefly described|Map Legend|Neoproterozoic III|Neoproterozoic III|Of the Kuniandi Group. Tillite, purple or cream laminated dolomite, sandstone, and siltstone. Age: c.610Ma. Geological Province: Louisa Basin.||||||26-MAY-05
27180|Landrigan Tillite|44397|14|Not recorded|p.19, Table 3||Adelaidean|Kuniandi Group. "Landrigan Formation" - Defn. on Tech.File E/52-9.||||||
27180|Landrigan Tillite|44398|14|Not recorded|map legend||Adelaidean|||||||
27180|Landrigan Tillite|45047|4|Described|p36|||See also pp38,40.||||||20-FEB-08
27180|Landrigan Tillite|48927|2|Defined|p10|Adelaidean|Adelaidean|||||||
27180|Landrigan Tillite|63458|5|Briefly described|p871-874, p877 Tb.1, p880-882, p891-901.|Cryogenian|Cryogenian|Mount Ramsay area, Kimberley region. Laminated dolomicrite unit probably deposited by turbidity currents. Overlies striated pavement. Isotopic and elemental composition of carbonate unit given. The 'cap dolomicrite' facies is dealt with in detail.||Unit in Kuniandi Group.||Is overlain by Stein Formation or Wirara Formation. A correlative of Walsh and Moonlight Valley Tillites.|Massive diamictite constitutes the bulk of the formation; overlain by 4-9 m thick pink-cream, thinly laminated dolostone.|
27180|Landrigan Tillite|63762|5|Briefly described|p19|||See also Landrigan Formation.||||||07-FEB-11
27180|Landrigan Tillite|64104|6|Mentioned|p63, p72|Neoproterozoic|Neoproterozoic|The author proposes this name be replaced by Landrigan Formation "to distinguish stratigraphic terms from genetic interpretation".||||||
27180|Landrigan Tillite|68276|6|Mentioned|p68, 73|Neoproterozoic|Neoproterozoic|Kimberley region. The ""Tillite"" is omitted.",,|||||Diamictite with a recognizable Marinoan-type cap dolostone.|
27180|Landrigan Tillite|68473|6|Mentioned|p530-531|||Mount Ramsay.||Duerdin Group||||
27180|Landrigan Tillite|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Kuniandi Group.|||Massive tillite with thick lenses of sandstone and siltstone, and capped with purple or cream flaggy laminated dolomite; erratics of sandstone, subarkose, stromatolitic dolomite, granite and dolerite in a purple clayey or sandy matrix|
68667|Langenbeck Suite|61253|5|Briefly described|p56,  p52 Fig. 2|Archean|Archean|Of the Sisters Supersuite. Widespread mafic-ultramafic sills and rocks with boninite-like compositions (Smithies 2002).  Intrusive equivalent of Bookingarra Group. Age: >2.9Ga.  Geological Province:  Pilbara Craton. See also p54-55 Fig. 3.||||||07-NOV-08
68667|Langenbeck Suite|63441|5|Briefly described|p12 tb. 2, p38|Archean|Archean|Includes Millindinna Complex now redefined as Millindinnah Intrusion, unnamed gabbro intrusions on SATIRIST, and Opaline Well Intrusion (SHERLOCK). Intrusive equivalent of Bookingarra Group. Layered mafic and ultramafic rocks. See also p33 Fig. 12||||||07-FEB-11
68667|Langenbeck Suite|63538|6|Mentioned|p6 Fig. 3|Archean|Archean|Geological Province: Pilbara Craton.||||||19-APR-13
68667|Langenbeck Suite|64632|6|Mentioned|p203|||Presumably Mesoarchean if intrusive equivalents of Booklingarra Formation basalts||||Intrusive equivalent of the Bookingarra Formation basalts.|LREE-enriched gabbro rocks.|
68667|Langenbeck Suite|66217|5|Briefly described|p43.|Mesoarchean|Mesoarchean|Mallina Basin. Hosts PGE and orthomagmatic gold deposits.|2955-2945 Ma.|Unit in Sisters Supersuite.|||Ultramafic-mafic intrusions.|
68667|Langenbeck Suite|67201|5|Briefly described|p7 Fig.4, p23-24|||West Pilbara Superterrane.||Sisters Supersuite|||Unusual LREE-enriched gabbroic rocks.|
68667|Langenbeck Suite|69185|5|Briefly described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Sisters Supersuite.|Incldues Millindinnah Intrusion, Opaline Well Intrusion.|||
68667|Langenbeck Suite|69301|5|Briefly described|p5 Fig.3|||Pilbara Craton. West Pilbara Superterrane.|||||Granitic rocks.|
68667|Langenbeck Suite|70022|6|Mentioned|p115|||West Pilbara Superterrane.||||||
68667|Langenbeck Suite|70775|5|Briefly described|iii, p10, p13|Mesoarchean|Mesoarchean|Mallina Basin. An age range of 2955-2940 is provided [though no source is given]. See also p29 tbl 5, p63-p64, p66, p77, p79.|c. 2950 Ma (Smithies et al 2007a)|Sisters Supersuite|Includes the Sherlock Intrusion.|||
68667|Langenbeck Suite|72034|6|Mentioned|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Millindinna Intrusion, Opaline Well Intrusion, Shay Intrusion, Sherlock Intrusion.|||
68667|Langenbeck Suite|72668|5|Briefly described|p4, p15-17|||West Pilbara Superterrane. Individual units vary geochemically except for surprisingly constant La/Sm and La/Zr ratios.  Intrusive equivalent of Bookingarra Group [sic - should be Formation in this paper]||Sisters Supersuite|||Unusual LREE enriched gabbro rocks.|13-JAN-22
27181|Langey Shale|7433|5|Briefly described|p43.|Jurassic|Jurassic|Informal name in pre-1970s literature.||Now included in Jarlemai Siltstone.|||Nodular phosphatic bed.|
27181|Langey Shale|32648|6|Mentioned|p32|||U. Jur.||||||
27181|Langey Shale|36890|3|Fully described|p348|||Formerly Langey Crossing Marl, Langey Slst.,&Langey Beds.||||||
27181|Langey Shale|37577|6|Mentioned|p67|||||||||
27181|Langey Shale|45153|2|Defined|App.6-122|Kimmeridgian|Kimmeridgian|Formerly Langey Crossing Marl,Langey Marl, Langey Siltstone, Langey Beds||||||
27460|Lansdowne Arkose|22547|4|Described|p21||Orosirian|Of the Speewah Group. Geological province: Speewah Basin. Thickness: 400 m. Overlies Valentine Siltstone.||||||14-NOV-06
27460|Lansdowne Arkose|22754|5|Briefly described|p10 Tb. 2|Paleoproterozoic|Paleoproterozoic|Of the Speewah Group.||||||07-NOV-08
27460|Lansdowne Arkose|23125|4|Described|Table.1, p389||Proterozoic|Age: Early Proterozoic. Of Speewah Group.||||||28-NOV-06
27460|Lansdowne Arkose|23751|4|Described|p21|Paleoproterozoic|Paleoproterozoic|Of Speewah Group. Geological Province: Speewah Basin. Max. thickness: 450 m.||||||07-NOV-08
27460|Lansdowne Arkose|30097|6|Mentioned|Table 23|||Also Tables 24,28||||||
27460|Lansdowne Arkose|30525|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27460|Lansdowne Arkose|30533|5|Briefly described|p15|||On Table 2||||||
27460|Lansdowne Arkose|30558|6|Mentioned|p36|||||||||
27460|Lansdowne Arkose|30894|5|Briefly described|p250|||Carpentarian||||||
27460|Lansdowne Arkose|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27460|Lansdowne Arkose|30896|4|Described|p16|||||||||
27460|Lansdowne Arkose|31404|6|Mentioned|Fig.1|||||||||
27460|Lansdowne Arkose|32660|5|Briefly described|Table 3|||||||||
27460|Lansdowne Arkose|32664|6|Mentioned|Map legend|Carpentarian|Carpentarian|Briefly described in notes||||||
27460|Lansdowne Arkose|36551|6|Mentioned|Table 10|||||||||
27460|Lansdowne Arkose|36885|4|Described|p186|||||||||
27460|Lansdowne Arkose|36902|6|Mentioned|p11|||||||||
27460|Lansdowne Arkose|37462|6|Mentioned|Fig.4.9|||||||||
27460|Lansdowne Arkose|38482|6|Mentioned|Table 1|||||||||
27460|Lansdowne Arkose|41987|5|Briefly described|Fig.4 P74|||||||||
27460|Lansdowne Arkose|42149|6|Mentioned|Table 1 P709|||||||||
27460|Lansdowne Arkose|42710|5|Briefly described|map legend|Proterozoic||||||||
27460|Lansdowne Arkose|42811|5|Briefly described|p21|||of Speewah Group||||||
27460|Lansdowne Arkose|43281|5|Briefly described|Map legend||Proterozoic|of Speewah Group.||||||
27460|Lansdowne Arkose|43853|5|Briefly described|Map Legend||Proterozoic|||||||
27460|Lansdowne Arkose|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
27460|Lansdowne Arkose|44230|5|Briefly described|Map Legend||Proterozoic|||||||
27460|Lansdowne Arkose|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Speewah Group.  Buff to pale pink, medium- to coarse-grained arkose and feldspathic sandstone, granule and pebble conglomerate, and silty shale. Age: c.1835Ma. Geological Province: Speewah Basin.||||||07-NOV-08
27460|Lansdowne Arkose|44317|4|Described|Table 2||Carpentarian|||||||
27460|Lansdowne Arkose|44318|14|Not recorded|map legend||Carpentarian|Carpentarian.||||||
27460|Lansdowne Arkose|44363|5|Briefly described|p.6,11,12,13|||(Carpentarian) Speewah Group.||||||
27460|Lansdowne Arkose|44364|14|Not recorded|map legend|||||||||
27460|Lansdowne Arkose|44366|14|Not recorded|p.13, Table 2||Carpentarian|Part of Speewah Group.||||||
27460|Lansdowne Arkose|44367|14|Not recorded|map legend||Proterozoic|(Reprinted 1971), part of Speewah Group.||||||
27460|Lansdowne Arkose|44397|14|Not recorded|p.9, Table 2||Carpentarian|Speewah Group.||||||
27460|Lansdowne Arkose|44398|14|Not recorded|map legend||Carpentarian|||||||
27460|Lansdowne Arkose|45047|5|Briefly described|p28|||||||||
27460|Lansdowne Arkose|48931|3|Fully described|p48|||||||||
27460|Lansdowne Arkose|60714|6|Mentioned|p113 Fig.2. |||||Unit in Speewah Group.||Overlies Valentine Siltstone. Is overlain by Luman Siltstone.||
27460|Lansdowne Arkose|64748|4|Described|p269 Fig 2, p271, 274-6, 278|||Of the Speewah Group; contains red beds; Underlies the Luman Siltstone; overlies the Valentine Siltstone; red-brown sandstone||||||
27460|Lansdowne Arkose|67563|5|Briefly described|p121, p122 Fig.2|Orosirian|Orosirian|Youngest detrital zircon population age of 1860 +/- 6 Ma (Kirkland et al. 2010).|1860 +/- 6 Ma|Of the Speewah Group.||||20-JAN-17
27460|Lansdowne Arkose|68078|4|Described|p5, p6 figure 3, p11, p14 figure 10|Paleoproterozoic|Paleoproterozoic|Age is maximum depositional age.|1860 Ma +/-6 Ma (SHRIMP)|Speewah Group||Overlies Luman Siltstone, Overlain by Valentine Siltstone|Arkose.|13-SEP-22
27460|Lansdowne Arkose|68992|5|Briefly described|p498 Fig.1, p499||Orosirian|Speewah Basin. Youngest detrital zircon age.|1860 +/- 6 Ma (Kirkland et al, 2010)|Of the Speewah group.||||21-JUL-15
27460|Lansdowne Arkose|69003|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|U-Pb zircon maximum depositional age.|<1860 Ma.|Speewah Group.||Overlies Valentine Siltstone. Is overlain by Luman Siltstone.||
27460|Lansdowne Arkose|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Speewah Basin. Age from analyses released in 2010. Note: age of felsic volcanics in underlying Valentine Siltstone is 1834+/-3 Ma. Age and unit relationships from geochron file 182106.1.pdf.|Max.deposit 1860+/-6 Ma U/Pb SHRIMP|Speewah Group|Includes unnamed member.|Conformably overlain by Luman Siltstone. Conformably overlies Valentine Siltstone. Intruded by Hart Dolerite.|Thin-bedded, purple-brown, grey, and white feldspathic sandstone with interbedded quartz sandstone; minor micaceous siltstone and mudstone.|31-JUL-15
27460|Lansdowne Arkose|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Speewah Group|||Thin-bedded, purple-brown, grey and white feldspathic sandstone with interbedded quartz sandstone; minor micaceous siltstone and mudstone. Thin to thickly bedded feldspathic quartz sandstone.|
27460|Lansdowne Arkose|69585|4|Described|p4-5, p8-9, p12, p15-16, p27|Orosirian|Orosirian|Western Lamboo Province. Fluvial succession with marine incursions. U-Pb and Lu-Hf isotope data and diagram.|1860 +/- 6 Ma (maximum depositional age).|Speewah Group.||Conformably overlies Valentine Siltstone. Is overlain conformably by Luman Siltstone.|Feldspathic sandstones and arkoses with interbedded medium- to coarse-grained quartz sandstones, with minor micaceous siltstones and claystones. Dominated by trough cross-stratification with cross-bed foresets up to 1m thick.|
27460|Lansdowne Arkose|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Speewah Basin, Kimberley Craton.||Unit in Speewah Group.|||Thin-bedded, purple-brown, grey, and white feldspathic sandstone with interbedded quartz sandstone; minor micaceous siltstone and mudstone.|
27460|Lansdowne Arkose|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Speewah Basin; North Australian Craton.||Speewah Group.||Overlies Valentine Siltstone. Is overlain by Luman Siltstone.|Thin-bedded, purple-brown, grey, and white feldspathic sandstone with interbedded quartz sandstone; minor micaceous siltstone and mudstone.|
27460|Lansdowne Arkose|70154|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic||1797-1835 Ma|Speewah Group|||Thin-bedded, purple-brown, grey, and white feldspathic sandstone with interbedded quartz sandstone; minor micaceous siltstone and mudstone. Mudstone, siltstone and thin- thick bedded feldspathic quartz sandstone.|
27460|Lansdowne Arkose|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen, King Leopold Orogen. Of Speewah Basin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyp_lut.csv and geochron files.|1835-1797 Ma (inferred)|Unit of Speewah Group.||Overlain conformably by Luman Siltstone. Underlain conformably by Valentine Siltstone.|Pink to red-brown, grey and green medium grained feldspathic sandstone with small scale cross beds, grading to arkose; lesser coarse poorly sorted sandstone and recessive green-red-brown micaceous siltstone, shale and phyllite|
27460|Lansdowne Arkose|71281|4|Described|p421-426, p428-432|Paleoproterozoic|Paleoproterozoic|Dow and Gemuts (1967). Speewah Basin. Up to 400m thick. Open-water to marine deposits. Contains sand dykes. Photo and photomicrograph. Zircon analyses detailed; provenance discussed. Youngest zircon is aged at 1836 +/- 23 Ma.|1861 +/- 6 Ma (maximum depositional age).|Speewah Group.||Conformably overlies Valentine Siltstone. Is overlain by Luman Siltstone.|Pink to red-brown, medium-grained feldspathic to arkosic sandstone with small cross-beds, less coarse poorly-sorted sandstone and green to brown micaceous siltstone, shale and phyllite. Common beds of clay-clast conglomerate.|
27460|Lansdowne Arkose|71784|6|Mentioned|p83||Proterozoic|Speewah Group.||||||
27460|Lansdowne Arkose|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Speewah Group.||Overlies Hart Dolerite. Is overlain by Bedford Sandstone.|Thin- to thick-bedded, cross-bedded feldspathic sandstone with interbedded micaceous siltstone and mudstone.|
27460|Lansdowne Arkose|72490|5|Briefly described|p3-5, p8, p10|||Maximum thickness of 400 m.||Speewah Group||Intruded by Hart Dolerite.|Pink to red-brown, medium-grained feldspathic to arkosic sandstone with small cross-beds, less coarse poorly-sorted sandstone and green to brown micaceous siltstone, shale and phyllite.|
79521|Larkinville Granodiorite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||3010 - 2600 Ma (inferred).||||Granodiorite; metamorphosed.|
79521|Larkinville Granodiorite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|3010-2600 Ma (inferred)||||Granodiorite; metamorphosed|
73328|Larranganni Formation|64277|5|Briefly described|Map ledgend|Mesozoic|Mesozoic|Geological Province: Canning Basin. Sandstone; minor siltstone and conglomerate.||||||
73328|Larranganni Formation|66129|5|Briefly described|p215 Fig.2|||Sandstone, siltstone, minor conglomerate, commonly silicified. Mesozoic?||||||
73328|Larranganni Formation|68474|5|Briefly described|p573|Mesozoic|Mesozoic|Granites-Tanami Orogen.|||||Sandstone, siltstone, shale, minor conglomerate; commonly silicified.|
73328|Larranganni Formation|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Mesozoic|Mesozoic|Canning Basin|||||Sandstone, minor siltstone, and conglomerate|
73328|Larranganni Formation|69587|5|Briefly described|GEOL_LUT_CSV files|Mesozoic|Mesozoic|Of Canning Basin. Events: Alice Springs Orogeny; Point Moody Extension; Prices Creek Movement; Red Bluffs Extension; Van Emmerick Extension. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|252.17-66 Ma (inferred)||||Sandstone, minor siltstone, and conglomerate|
73328|Larranganni Formation|70141|5|Briefly described|Map legend.|Mesozoic|Mesozoic|Canning Basin.|||||Sandstone, minor siltstone and conglomerate.|
73328|Larranganni Formation|70143|5|Briefly described|Map legend|Mesozoic|Mesozoic|Canning Basin.|||||Sandstone, minor siltstone and conglomerate.|
73328|Larranganni Formation|70154|5|Briefly described|500k_interpgeop14_lut.csv|Mesozoic|Mesozoic||66-251 Ma||||Sandstone, minor siltstone, and conglomerate|
73328|Larranganni Formation|70826|6|Mentioned|p7 tbl 4|Mesozoic|Mesozoic|Eastern Canning Basin.||||||
73328|Larranganni Formation|70852|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Sandstone, minor siltstone and conglomerate, poorly sorted, quartz-rich.|
73328|Larranganni Formation|71267|4|Described|GEOL_LUT_CSV files|Mesozoic|Mesozoic|Of Canning Basin. Events: Point Moody Extension (300-242 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|252.17-66 Ma (inferred)||||Medium grained and thin to medium bedded fluvial quartz sandstone with minor siltstone and conglomerate|
73328|Larranganni Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesozoic|Mesozoic|Canning Basin.|||||Sandstone, minor siltstone, and conglomerate.|
22169|Larry Formation|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Rudall Complex, Paterson Orogen.||||||
22169|Larry Formation|23602|4|Described|p9|||Of Rudall Complex. Overlying unit Fingoon Quartzite. Max. thickness: >1000 m.||||||
22169|Larry Formation|23760|4|Described|p14|Proterozoic|Proterozoic|Geological Province: Talbot Terrane.||||||
22169|Larry Formation|43848|5|Briefly described|Map Legend||Proterozoic|||||||
22169|Larry Formation|64580|6|Mentioned|map legend|||Quartzite, psammitic paragneiss, banded paragneiss, and pelitic schist.||||||15-DEC-08
22169|Larry Formation|64943|4|Described|p4-6, p8-9,10,11,13,20,24,27,28,38|Orosirian|Paleoproterozoic|Talbot Terrane, Rudall Complex. >1000m; dominantly quartz-feldspar-muscovite paragneiss with quartz-mica schist and minor muscovitic quartzite; min deposition age 1801+/-4 Ma; type locality given. Transitional contact with overlying Fingoon Quartzite||||||
22169|Larry Formation|65454|6|Mentioned|p4, p30 Fig.A1b|Statherian|Statherian|Of Fingoon Package, Talbot Terrane. Age uncertain but experienced Yapungku Orogeny ~1800-1760 Ma or ~1680 Ma, and an earlier event?||||||21-APR-16
22169|Larry Formation|67202|5|Briefly described|p56|||Talbot Terrane, Rudall Complex. Unknown thickness.|||||Quartz-feldspar-mica paragneiss and quartz-mica schist.|
22169|Larry Formation|68981|5|Briefly described|p2|||Eastern Talbot Terrane, Rudall Province.||||Is overlain conformably by Fingoon Quartzite.|Quartz-feldspar-mica paragneisses.|
22169|Larry Formation|71169|5|Briefly described|v, p3-p6, p18|Statherian|Statherian|Locally preserves cross-bedding and graded bedding that youngs towards the Fingoon Quartzite. It is unclear whether the U-Pb zircon age represents the maximum or minimum depositional age for this unit. See also p22-p24, p59-p60, p65, p67, p70.|1760 +/- 5 Ma (U-Pb zircon)|||Structurally overlain by the Fingoon Quartzite.|Quartz-feldspar-mica paragneiss and schists.|
22169|Larry Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||pelite, quartzite, psammite, gneiss|
22169|Larry Formation|71795|6|Mentioned|p35 fig 4|||Rudall Province.||||||
22169|Larry Formation|73168|6|Mentioned|p741 Fig.2, p742|Mesoproterozoic|Paleoproterozoic|Rudall Province. Talbot Domain, eastern. Deposited after 1760 +/- 5 Ma. Interpreted to represent a syn- or post-magmatic cover sequence derived from the Kalkan Supersuite.||||||
69749|Latitude Hill Gabbro|61340|5|Briefly described|Map legend|||Presented as the compound name Latitude Hill Gabbro/Pyroxenite Intrusion.  Together with the Latitude Hill Pyroxenite, stated to be a segment of the Michael Hills gabbro.||||||21-SEP-05
69750|Latitude Hill Pyroxenite|61340|5|Briefly described|Map legend|||Presented as the compound name Latitude Hill Gabbro/Pyroxenite Intrusion.   Together with the Latitude Hill Gabbro, stated to be a segment of the Michael Hills gabbro.||||||21-SEP-05
79621|Latitude Hills intrusion|68996|5|Briefly described|p45, p50, 51, 57,62, 63, 64, 65|Mesoproterozoic|Mesoproterozoic|Part of G1 group. Along with Michael Hills intrusion, characterised by very strong aeromagnetic anomalies.||Giles Suite||||
23718|Lauchie Member|42615|4|Described|p33|||Of Eliasson Formation. Reserved.||||||29-NOV-06
25727|Laurel Formation|13255|6|Mentioned|p368|Early Carboniferous|Early Carboniferous|Oobagooma Sub-basin, Roebuck Basin.||||Overlies Pillara Reef Complex. Is overlain by Anderson Formation.||
25727|Laurel Formation|22741|5|Briefly described|P24, Table3 P15||Early Carboniferous|||||||
25727|Laurel Formation|22764|4|Described|Table2,p10||Early Carboniferous|Fairfield Group. 1000 m.||||||01-FEB-10
25727|Laurel Formation|22776|4|Described|Table.3|Early Carboniferous|Late Devonian|Of the Fairfield Group. Fossil assemblage includes brachiopods, conodonts, corals and nautiloids.||||||13-NOV-07
25727|Laurel Formation|23293|2|Defined|p21|Early Carboniferous|Early Carboniferous|First named Laurel Beds by Thomas (1957).||||||
25727|Laurel Formation|23294|14|Not recorded|p45||Early Carboniferous|Has yielded ostracods.||||||
25727|Laurel Formation|23523|5|Briefly described|p1001 Fig.2|Carboniferous|Carboniferous|||||||
25727|Laurel Formation|23766|5|Briefly described|p15|Early Carboniferous|Late Devonian|Of the Fairfield Group.||||||13-NOV-07
25727|Laurel Formation|24061|4|Described|p181|Early Carboniferous|Early Carboniferous|Geological Province: Canning Basin. Maximum thickness: 1981m.||||||03-FEB-10
25727|Laurel Formation|24062|5|Briefly described|p186 Table 1|Carboniferous|Carboniferous|Geological Province: Canning Basin.||||||
25727|Laurel Formation|24246|5|Briefly described|p9, 12, 14|Early Carboniferous|Early Carboniferous|Geological Province: Canning Basin.||||||24-FEB-05
25727|Laurel Formation|24370|5|Briefly described|p39|||Geological Province: Canning Basin.||||||
25727|Laurel Formation|24390|5|Briefly described|p8|Carboniferous|Carboniferous|Geological Province: Canning Basin. Of the Fairfied Group.||||||03-FEB-10
25727|Laurel Formation|29813|6|Mentioned|p17|||||||||
25727|Laurel Formation|29818|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25727|Laurel Formation|30110|6|Mentioned|p81|||See also P83. Visean age.||||||
25727|Laurel Formation|30595|5|Briefly described|p3|||||||||
25727|Laurel Formation|30897|4|Described|p18|||||||||
25727|Laurel Formation|32376|6|Mentioned|p1541|||||||||
25727|Laurel Formation|32865|6|Mentioned|p475|||Early Carb. fauna||||||
25727|Laurel Formation|33518|4|Described|Table 1|||||||||
25727|Laurel Formation|33519|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25727|Laurel Formation|33960|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25727|Laurel Formation|33965|6|Mentioned|p13|||||||||
25727|Laurel Formation|34085|6|Mentioned|Cor.chart|||Tournaisian||||||
25727|Laurel Formation|35120|6|Mentioned|Map legend|Early Carboniferous|Middle Devonian|||||||
25727|Laurel Formation|35124|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25727|Laurel Formation|35275|6|Mentioned|Fig.5.|||||||||
25727|Laurel Formation|36224|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Of the Fairfield Group.  Limestone, shale, siltstone; sandstone. Late Devonian to Early Carboniferous.||||||29-NOV-06
25727|Laurel Formation|36225|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Late Devonian to Early Carboniferous||||||
25727|Laurel Formation|36331|6|Mentioned|p56|||||||||
25727|Laurel Formation|36890|6|Mentioned|p335|||Included in Fairfield Formation||||||
25727|Laurel Formation|38277|6|Mentioned|p154|||||||||
25727|Laurel Formation|40838|6|Mentioned|p278|||||||||
25727|Laurel Formation|40866|6|Mentioned|p181|||||||||
25727|Laurel Formation|41023|4|Described|p288|||||||||
25727|Laurel Formation|41169|6|Mentioned|p148|||||||||
25727|Laurel Formation|41215|6|Mentioned|p278|||||||||
25727|Laurel Formation|41217|6|Mentioned|p310|||||||||
25727|Laurel Formation|41593|6|Mentioned|p3|||||||||
25727|Laurel Formation|41730|6|Mentioned|p472|||See also p486.||||||28-JAN-20
25727|Laurel Formation|41839|3|Fully described|p21|||Formerly "Laurel Beds".||||||13-NOV-07
25727|Laurel Formation|42030|5|Briefly described|p747|||||||||
25727|Laurel Formation|42032|6|Mentioned|p513|||||||||
25727|Laurel Formation|42347|6|Mentioned|Fig.2 P1020|||||||||
25727|Laurel Formation|42547|4|Described|p92|||||||||
25727|Laurel Formation|42564|6|Mentioned|p11|||Fairfield Group.||||||
25727|Laurel Formation|42811|6|Mentioned|p43|||of Fairfield Group||||||
25727|Laurel Formation|42860|5|Briefly described|Fig.2|||||||||
25727|Laurel Formation|42880|5|Briefly described|Fig.2,p1020|||||||||
25727|Laurel Formation|42930|5|Briefly described|Fig.1 p473|Early Carboniferous|Early Carboniferous|Conformably overlies Nullara and Windjana Limestones; conformably underlies Anderson Formation. Geological Province: Canning Basin.||||||13-NOV-07
25727|Laurel Formation|42933|5|Briefly described|Fig.94 p258|||||||||
25727|Laurel Formation|42994|6|Mentioned|p13|||||||||
25727|Laurel Formation|43173|6|Mentioned|15-54||Early Permian|||||||
25727|Laurel Formation|43563|6|Mentioned|Fig.5,p10||Early Carboniferous|||||||
25727|Laurel Formation|43666|6|Mentioned|p23||Early Carboniferous|||||||
25727|Laurel Formation|43815|6|Mentioned|p93|||||||||
25727|Laurel Formation|43818|6|Mentioned|Table 2,p42|||||||||
25727|Laurel Formation|43825|6|Mentioned|p144||Carboniferous|||||||
25727|Laurel Formation|43932|5|Briefly described|p4,Tb.1 p7|||||||||
25727|Laurel Formation|44040|14|Not recorded|p43|||||||||
25727|Laurel Formation|44100|14|Not recorded|p41|||||||||
25727|Laurel Formation|44143|4|Described|p.437 Table 4-19|Carboniferous|Devonian|Unit in Fairfield Group. Up to 650m thick; limestone and sandstone; shallow marine. Conformable on Yellow Drum Sandstone. Type section in two sections: details given. Contains algae, brachiopods, bryozoans, bivalves, ostracods, microflora and conodonts: Tournaisian.||||||
25727|Laurel Formation|44356|5|Briefly described|p9,Tb.1 p7||Early Carboniferous|||||||
25727|Laurel Formation|44993|14|Not recorded|p.7,11,40|||Camaratoechia.||||||
25727|Laurel Formation|44994|5|Briefly described|p11|||Fig.6 Correlation. Lower Carboniferous.||||||13-NOV-07
25727|Laurel Formation|44998|2|Defined|p61||Tournaisian|Late Tournaisian. Probably overlies Fairfield Beds. Overlain by Grant Formation. See also p42,62,map,App.3 p277-280.||||||
25727|Laurel Formation|45015|6|Mentioned|p66|||Can be correlated with Moogooree Limestone. Geological Province: Fitzroy Basin.||||||29-NOV-06
25727|Laurel Formation|45063|6|Mentioned|p29|||See also P30 & Fig. 9. Carb.||||||
25727|Laurel Formation|45097|4|Described|p7|||Brachiopods. See also p21, 22 and Correlation chart.||||||13-NOV-07
25727|Laurel Formation|45101|6|Mentioned|p1|||||||||
25727|Laurel Formation|45133|4|Described|p2|||||||||
25727|Laurel Formation|45143|1|Redefined|p24|Tournaisian|Tournaisian|||||||
25727|Laurel Formation|45153|1|Redefined|App.3-42|Tournaisian|Tournaisian|||||||
25727|Laurel Formation|45158|4|Described|p22|||||||||
25727|Laurel Formation|45169|6|Mentioned|p13|||||||||
25727|Laurel Formation|46794|5|Briefly described|p64|||||||||
25727|Laurel Formation|46849|6|Mentioned|p182|||||||||
25727|Laurel Formation|46856|6|Mentioned|p272|||||||||
25727|Laurel Formation|48573|14|Not recorded|p.2,3,5,9,15-17,20|||(E51-7/Alexander Creek) Tb.3,22.||||||
25727|Laurel Formation|48831|14|Not recorded|p.60|||||||||
25727|Laurel Formation|48837|2|Defined|p.21-28|||On many pages. p.18,21-28,30,34.||||||
25727|Laurel Formation|48848|14|Not recorded|p.62|||||||||
25727|Laurel Formation|48971|6|Mentioned|p10|||See also P15,30,32,33,34,35,37,39,40,41,42,43.||||||
25727|Laurel Formation|48978|4|Described|p4|||Geochemistry p11, etc.||||||13-NOV-07
25727|Laurel Formation|50085|5|Briefly described|p8|Early Carboniferous|Early Carboniferous|Of the Fairfield Group.  Geological Province: Canning Basin.||||||
25727|Laurel Formation|60364|5|Briefly described|p208|Carboniferous|Devonian|Contains ostracods. Geological Province: Canning Basin||||||
25727|Laurel Formation|61551|6|Mentioned|p355, p359, p361. |Early Carboniferous|Early Carboniferous|Canning Basin. Hydrocarbon source rocks for suprasalt plays. Oil sourced from this unit is produced from the Anderson Formation at Lloyd and West Kora fields. Is also referred to as Upper Carboniferous in the article.||||||
25727|Laurel Formation|64187|5|Briefly described|p320 Fig. 2|Tournaisian|Famennian|Underlain unconformably by Luluigui Formation and Yellow Drum Formation, overlain by Anderson Formation. Carbonate, shale, siltstone (marine). Geological Province: Canning Basin.||||||03-FEB-10
25727|Laurel Formation|64580|6|Mentioned|map legend|||Of Fairfield Group.||||||15-DEC-08
25727|Laurel Formation|64643|5|Briefly described|p3 Fig. 2|Missippippian|Missippippian|||||||
25727|Laurel Formation|64694|6|Mentioned|p233, p253|Tournaisian|Tournaisian|Canning Basin. Contains Grandispora species, also found in Sorby Dolomite Member.||||Is correlated with Langfield Group.||
25727|Laurel Formation|64971|6|Mentioned|p685, p689 Fig. 2|Early Carboniferous|Early Carboniferous|||||||09-FEB-10
25727|Laurel Formation|64981|5|Briefly described|p667, p670, p677.|Famennian|Famennian|First well drilled on Lennard Shelf, in 1958, recovered a few gallons of oil from this unit. Potential source rock for Sundown oil field. Gas was recovered from Meda 1 drill.||Unit in Fairfield Group.||Overlies Yellow Drum Formation. Is overlain by Anderson Formation.|Shallow marine muds and carbonates.|
25727|Laurel Formation|65301|5|Briefly described|p5 Fig. 4|Mississippian|Mississippian|Of Fairfield Group. Geological province: Canning Basin.||||||
25727|Laurel Formation|65449|6|Mentioned|p6|Early Carboniferous|Early Carboniferous|||Fairfield Group.||||
25727|Laurel Formation|66127|5|Briefly described|Plates 3, 4, 7.|Tournaisian|Tournaisian|||Unit in Fairfield Group||Overlies Yellow Drum Sandstone.|Marine limestone, shale, siltstone and sandstone.|
25727|Laurel Formation|66498|6|Mentioned|p46|Carboniferous|Carboniferous|Canning Basin. Contains a rich and diverse micro- and macro-vertebrate fossil assemblage (described).||||||
25727|Laurel Formation|67131|6|Mentioned|p2, p3 Fig. 2|Tournaisian|Tournaisian|||Of Fairfield Group||Overlies Yellow Drum Sandstone.||28-JAN-20
25727|Laurel Formation|68007|6|Mentioned|p4|Early Carboniferous|Early Carboniferous|Canning Basin.||||||25-FEB-20
25727|Laurel Formation|68902|5|Briefly described|p9 fig 5|Carboniferous|Carboniferous|||Fairfield Group||Overlies Yellow Drum Formation; overlain by Anderson Formation.||
25727|Laurel Formation|69029|5|Briefly described|p313,321-322,333|Early Carboniferous|Early Carboniferous|Of Canning Basin. Comprises lower reef complexes deposited during major Frasnian transgression. Source rocks can be correlated to oil discovered on the margins of the Fitzroy Trough. Source rocks generated oils to the Boundary, Lloyd, Sundown, and West Terrace oil fields (Lennard Shelf, southern margin Fitzroy Trough). Also acts as both source and reservoir to oil and gas discoveries in the Yulleroo and Ungani areas.||||||
25727|Laurel Formation|69099|5|Briefly described|500k_geologyp08_lut.csv|Tournasian|Famennian|||Fairfield Group||||
25727|Laurel Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Tournaisian|Famennian|||||||
25727|Laurel Formation|69182|6|Mentioned|Ch4 p9, Ch4 p13-p14|Tournaisian|Tournaisian|North Canning Basin. Can reach thicknesses in excess of 1000m in the Fitzroy depocentre. Potential seal for the storage of carbon dioxde. See also Ch4 p30-p36, Ch4 p38, Ch4 p42, Ch4 p44, Ch4 p45, Ch4 p47, Ch4 p50-p58, Ch4 p74-p77, Ch4 p84, Ch4 p86, Ch4 p88, Ch4 p90-p91.||Fairfield Group||Overlies the Yellow Drum Formation.||
25727|Laurel Formation|69206|6|Mentioned|p2|Carboniferous|Carboniferous|Canning Basin. The source of oil recovered from the Lennard Shelf.||||||
25727|Laurel Formation|69297|5|Briefly described|p337, p351, p352, p354, p355|Tournaisian|Tournaisian|Broome Platform of the Canning Basin and Canning Basin. May contain potential petroleum source and seal rocks. ||Fairfield Group||Overlies the Yellow Drum Sandstone; unconformably overlies the Pilara Sequence. Unconformably overlain by the Reeves Formation.||
25727|Laurel Formation|69312|4|Described|p1, p3, p9, p15, p19|Early Carboniferous|Early Carboniferous|Canning Basin. Contains oil-prone source rocks and has a TOC of up to 4 percent. Misspelt as the Laural Formationon p15. Up to 2695m thick. One of the three petroleum systems that forms the Larapintine Petroleum Supersystem. See also p23 fig 27, p24 fig 29, p25 fig 31, p27, p28 fig 35, p29, p29 fig 37, p30, p31. ||Fairfield Group|Includes the Laurel Shale and Laurel Sandstone.|Overlies the Yellow Drum Formation. Overlain by the Anderson Formation. Equivalent to the Luluigui and Clanmeyer Formations.|Interbedded shale, siltstone, sandstone and minor limestone.|11-FEB-20
25727|Laurel Formation|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Fairfield Group.||||
25727|Laurel Formation|69693|6|Mentioned|p3-4|Carboniferous||||Fairfield Group||||
25727|Laurel Formation|70065|5|Briefly described|Rowley: Fig.2. Regional: Fig.4; p6|Tournaisian|Tournaisian|Offshore Canning Basin. Basal marine shales have fair to good petroleum generative potential, and are inferred to be present throughout the Oobagooma Sub-basin. Believed to be the source of hydrocarbon accumulations in the overlying Grant Group.||Fairfield Group.||Overlies Pillara Limestone (Reef Complex). Is overlain by Grant Group.||
25727|Laurel Formation|70492|5|Briefly described|p166, 174, 181|Early Carboniferous|Early Carboniferous|Canning Basin. Sequence (stratigraphy) development diagram.||Fairfield Group.||Overlies Yellow Drum Formation. Is overlain by Anderson Formation.|A lower limestone unit and an upper siltstone unit with minor dolostone.|
25727|Laurel Formation|70774|5|Briefly described|p4|Mississippian|Mississippian|Fitzroy Trough and Lennard Shelf, Canning Basin.||Fairfield Group||Overlies the Yellow Drum Formation. Overlain by the Anderson Formation.||
25727|Laurel Formation|71146|6|Mentioned|p12 fig 8, p44|Carboniferous|Devonian|Canning Basin.|ca 359 Ma|||||
25727|Laurel Formation|71233|5|Briefly described|p103|Tournaisian|Tournaisian|Canning Basin sub-surface. Age relations with NSW microflora discussed.||||||
25727|Laurel Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Fairfield Group.|||Shallow marine fossiliferous interbedded limestone, shale, siltstone and sandstone|
25727|Laurel Formation|71870|6|Mentioned|p1|Early Carboniferous|Early Carboniferous|Canning Basin. A petroleum source interval formed during the Larapintine petroleum supersystem.||||||28-JAN-20
25727|Laurel Formation|71894|5|Briefly described|p4|Tournaisian|Tournaisian|Canning Basin.||Fairfield Group||Overlies the Yellow Drum Formation. Unconformably overlain by the Anderson Formation.|Carbonate and shale.|
25727|Laurel Formation|72496|6|Mentioned|p226|||Identified as having high amplitude seismic facies. Thickens significantly within the hangingwall of the Harvey-Pinnacle fault.||||||
25727|Laurel Formation|72499|5|Briefly described|p7 Fig.6.|Tournaisian|Tournaisian|Located in the Fitzroy Trough.||Fairfield Group||Overlies Yellow Drum Formation and underlies Anderson Formation.|Includes carbonate shale.|
25727|Laurel Formation|72502|4|Described|p1-6, p8-21, p23|mid-Tournaisian|mid-Tournaisian|Lennard Shelf, Canning Basin. Poorly exposed in a 2-10 km wide belt southwest of the Napier and Oscar Ranges, with somewhat better exposures in the vicinity of Twelve Mile Bore. Well bedded limestones with vertebrate remains recovered mostly from crinoidal grainstones. Lagoonal and shallow ramp/shallow water carbonate platform facies. Contains a diverse fauna including bryozoans and corals, foraminifera, ostracods, rare ammonoids, and fish. Yielded a chondrichthyan fauna including Thrinacodus ferox, Cladodus thomasi, Protacrodus aequalis and Deihim mansureae. Assemblage comprises 16 taxa [article includes detailed systematic palaeontology]. Previous works described a rich shark assemblage. Age based on studies of the brachiopod and conodont faunas. Article compared shark fauna with chondrichthyan biofacies model by Ginter (2000).||Fairfield Group|||Characterised by a series of interbedded fossiliferous calcarenite, siltstone, sandstone and minor dolomitic beds.|
25727|Laurel Formation|72504|6|Mentioned|Figure 1-2|||Overlain by Grant Group in Lake Betty 1? Overlain by Anderson Formation in Bindi 1?||||||18-MAR-20
25727|Laurel Formation|73117|5|Briefly described|[See comments].|Tournaisian|Tournaisian|Hydrocarbon source rock that contributed to oil reservoired in the Reeves Formation and Grant Group. Contains local unnamed upper and lower limestone members. p: 1, 3, 16-17, 19, 21, 28, 32, 39, 109-110, 113, 120, 123, 125-126, 129-130, 135-140.||Fairfield Group||Underlain by Clanmeyer Formation. Unconformably overlain by Reeves Formation and Grant Group.|Mostly mudstone with thin carbonate and sandstone beds.|
77527|Laverton Sequence|63980|5|Briefly described|p57.|Archean|Archean|In this study, refers to Association 1 of Hallberg (1985): a succession of c.2.8 Ga komatiites, komatiitic basalts and tholeiites. Seems to be equivalent to Laverton Terrane of Myers, 1997.||||Is overlain by Kurnalpi Sequence.||15-DEC-14
77527|Laverton Sequence|66880|4|Described|p9, p18, pp27-28. |Archean|Archean|Term used in this study for the mafic to ultramafic volcanic succession of the Margaret Anticline, west of Laverton. Autochthonous basement to Kurnalpi Sequence.|2808 +/- 8 Ma.||||Mostly high-Ti tholeiitic basalt, komatiite, komatiitic basalt and banded iron formation; minor quartz-bearing clastic sedimentary rocks including turbidites; intruded by felsic porphyries.|
77527|Laverton Sequence|66937|6|Mentioned|p166.|Archean|Archean||c.2810 Ma.|||Is unconformably overlain by Wallaby Conglomerate, and thrust interleaved with White Hills Supersequence.||
77527|Laverton Sequence|67198|5|Briefly described|p4, p7, p46, p47-48|Neoarchean|Mesoarchean|Kositcin et al. (2008). Includes the oldest rocks in the Laverton region, Kurnalpi Terrane. The base is defined by BIF and ultramafic sequences that host the Windarra and Windarra South nickel sulfide deposits.|2808 +/- 8 Ma.|||Unconformably overlain by Kurnalpi Sequence|Mafic to ultramafic rocks: BIF and ultramafic sequences, overlain by basalt with gabbro and dolerite dykes, then more BIF, basalt and sedimentary sequences including interlayered volcaniclastic turbidite.|11-SEP-17
28672|Lawford Formation|41751|6|Mentioned|p8|||||||||
28672|Lawford Formation|43818|6|Mentioned|Fig.2.p39||Cenozoic|||||||19-NOV-08
28672|Lawford Formation|44143|4|Described|p.429 Table 4-19; p.452, Figure 4-113|Cainozoic|Cainozoic|Up to 24 m thick; calcrete, marl, sandy calcrete, and calcareous sandstone; fluvial. Unconformably overlies Grant Group, Noonkanbah Formation and Liveringa Group. Type section 15 km NE of Bulka Hills on tributary of Christmas Creek. Contains stromatolites and fossil wood.||||||
28672|Lawford Formation|44231|5|Briefly described|Map Legend||Tertiary|Limestone, calcareous siltstone, silicified limestone, and chalcedony.||||||26-MAY-05
28672|Lawford Formation|65829|6|Mentioned|p31.|||Kimberley area. Resembles Oakover Formation.||||||
28672|Lawford Formation|66127|5|Briefly described|Plates 4, 5, 7.|Miocene|Miocene||||||Crudely-bedded lacustrine siltstone, sandstone and chalcedonic limestone.|
28672|Lawford Formation|67860|4|Described|p418 Tb. 4-18|Cenozoic|Cenozoic|Up to 10m thick. Type section in tributary of Christmas Creek 15 km NE of Bullea Hills (Mount Bannerman). Unfossiliferous.||||Overlies Antrim Plateau Volcanics unconformably.|Limestone and chalcedony.|
28672|Lawford Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Lacustrine and fluvial calcrete, marl, sandy calcrete, calcareous sandstone, chalcedony, calcareous breccia and calcareous conglomerate; fossil wood and stromatolites in places and partly lateritised|
75111|Leake Spring Metamorphics|65453|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Under Yilgatherra Formation; intruded by Moorarie Supersuite and Durlacher Supersuite. Age: < c. 1960 Ma. Geol. Prov: Gascoyne Province.||||||
75111|Leake Spring Metamorphics|66105|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. 1842-1807 Ma. Map area shows four unnamed units; lithologies dominantly pelitic and psammitic schists, with calc-silicate gneiss, minor metasandstone, and granule metaconglomerate. ||||||
75111|Leake Spring Metamorphics|66110|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Comprises several unnamed units aged 1842-1807 Ma. Lithologies include a variety of schists, gneisses, amphibolites and metamorphosed siliciclastic rocks.||||||
75111|Leake Spring Metamorphics|66241|5|Briefly described|p9, p29.|||Gascoyne Province. Formerly Morrissey Metamorphics. Contains a well-developed medium-grade crenulation schistosity from an event dated c.1280 - 1250 Ma.||||||
75111|Leake Spring Metamorphics|66299|4|Described|pp3-5, pp121-145, p215.|Paleoproterozoic|Paleoproterozoic|Formerly part of the Morrissey Metamorphic Suite (Williams et al. 1979), and later the Morrissey Metamorphics (Martin et al. 2006); both terms are no longer valid. Medium-grained, mainly siliciclastic, metasedimentary rocks. Grades northwards into lower grade metamorphics of Ashburton Formation. Intruded by granites of Moorarie, Durlacher and Thirty Three Supersuites.|From 1842 +/- 5 Ma  to 1807 +/- 3 Ma.|||Unconformably overlies Middle Spring Granite and structurally overlies Halfway Gneiss. Is unconformably overlain by Pooranoo Metamorphics, Edmund Group and Mount Augustus Sandstone.|Psammitic and pelitic schists, commonly interlayered; lesser amphibolite; minor calc-silicate rock, chert, ultramafic schist, and metamorphosed banded iron-formation.|
75111|Leake Spring Metamorphics|66887|5|Briefly described|p3 Fig.2, p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Southern Gascoyne Province.|~1845-~1820 Ma estimated from Fig.4.|||||
75111|Leake Spring Metamorphics|66950|5|Briefly described|p3 Fig.2, p4, p7, pp9-17, p19, p25|Orosirian|Orosirian|Gascoyne Province. Originally known as the "Morrissey Metamorphic Suite" (Williams et al. 1978, 1983; Williams, 1986) and subsequently replaced by the "Morrissey Metamorphics" (e.g. Martic et al. 2007, 2008; Sheppard et al. 2008).|c. 1840-1820 Ma|||Intruded by the Moorarie Supersuite.|Dominated by pelitic and psammitic schists, with minor amounts of quartzite and calc-silicate rock. Amphibolite lenses and layers up to a few metres thick are a minor component of the succession.|16-DEC-16
75111|Leake Spring Metamorphics|67843|6|Mentioned|p2 Fig.1. |Paleoproterozoic|Paleoproterozoic|||||||
75111|Leake Spring Metamorphics|67888|6|Mentioned|p52|||Previously called the Morrissey Metamorphics||||||
75111|Leake Spring Metamorphics|68522|5|Briefly described|Map Legend|Orosirian|Orosirian|Gascoyne Province. 8 facies are mapped separately.|1840-1810 Ma||||Schists, gneiss, amphibolite.|
75111|Leake Spring Metamorphics|68981|5|Briefly described|p20-22|||Sheppard et al. (2010). Gascoyne Province. Deposition associated with the 1820-1770 Ma Capricorn Orogeny.|1840-1810 Ma.||||A package of low- to medium-metamorphic grade siliciclastic metasedimentary rocks.|
75111|Leake Spring Metamorphics|69003|5|Briefly described|p4, p25-26, p41|Paleoproterozoic|Paleoproterozoic|Gascoyne Province, Capricorn Orogen. Metamorphosed in the amphibolite facies by the 1385-1200 Ma Mutherbukin Tectonic Event.|1840-1810 Ma.|||||
75111|Leake Spring Metamorphics|69011|5|Briefly described|Map legend|Orosirian|Orosirian|Gascoyne Province. Nine facies are mapped separately.|1840-1810 Ma||||Includes schist, metasandstone and metaconglomerate, gneiss, and quartzite.|24-APR-14
75111|Leake Spring Metamorphics|69028|5|Briefly described|Map Legend|Orosirian|Orosirian|Gascoyne Province.|1840-1810 Ma||||Pelitic and psammitic schist; calc-silicate rock; minor amphibolite.|
75111|Leake Spring Metamorphics|69080|5|Briefly described|p684, p689, p697|Orosirian|Orosirian|Gascoyne Province. Forms kilometre-scale, highly planar, seismically-reflective rafts within the Minnie Creek batholith of the Moorarie Supersuite.|1840-1810 Ma.||||Pelitic and psammitic schist; calc-silicate rock; minor amphibolite.|
75111|Leake Spring Metamorphics|69166|5|Briefly described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Age derived from quartzite sample (190666.1.pdf)|1982 Ma +/- 9 Ma (SHRIMP)||||Pelitic, semipelitic and psammitic schist and gneiss; minor metasandstone and granule metaconglomerate, calc-silicate gneiss and schist. Actinolite-plagioclase schist;amphibolite.|
75111|Leake Spring Metamorphics|69387|5|Briefly described|p3,p7-8,p13,p15-23,p25-28, p30-35,p66|Orosirian|Orosirian|Mutherbukin Zone, Gascoyne Province. Locally, formerly mapped as Morrissey Metamorphics. Underwent medium-grade metamorphism and intrusion during the 1030-955 Ma Edmundian Orogeny. Deformations discussed; structural fabric diagrams. SG and magnetic susceptibility values given. Gravity and magnetic modelling. Appears as Leake Springs Formation [?] on p66.|1840-1810 Ma.|||Is intruded by the Thirty Three Supersuite.||
75111|Leake Spring Metamorphics|69596|6|Mentioned|p5|Orosirian|Orosirian|Gascoyne Province.||||||
75111|Leake Spring Metamorphics|70019|5|Briefly described|p94|Orosirian|Orosirian|Geological province: Gascoyne Province, Capricorn Orogen. Comprises Neoarchean to Paleoproterozoic basement rock assemblage of the Gascoyne Province. Package of medium- to high-grade metasedimentary rocks.|1840-1810 Ma|||||
75111|Leake Spring Metamorphics|70127|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Six un-named facies are mapped separately.|1842-1807 Ma.||||Calc-silicate gneiss and schist; pelitic and psammitic schists; quartzites; minor metasandstone and granule metaconglomerate.|
75111|Leake Spring Metamorphics|70138|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|1842-1807 Ma.||||Pelitic and psammitic schist, amphibolite, quartzite, actinolite schist after ultramafic rock.|
75111|Leake Spring Metamorphics|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 2_5m_interpgeop15_lut.csv, 100k_geologyl_lut.csvk, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv|1842-1807 Ma|||Intruded by Moorarie Supersuite|Pelitic and psammitic schist, gneiss, semipelitic schist, metamorphosed banded iron formation, calc-silicate gneiss and schist, amphibolite, actinolite and actinolite-plagioclase schist, metachert.|
75111|Leake Spring Metamorphics|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|Central Capricorn Orogen. May be a time equivalent of the Miningarra Group.||||||
75111|Leake Spring Metamorphics|71273|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||1842-1807 Ma.||||Recrystallised quartzite, sericitic quartzite, psammitic and pelitic schists, minor metasandstone and granule metaconglomerate.|
75111|Leake Spring Metamorphics|71869|6|Mentioned|p4|||Capricorn Orogen.||||||
75111|Leake Spring Metamorphics|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Gascoyne Province, Capricorn Orogen.||Max age ~1842 Ma, Min age 1807+/-3 Ma.|||Pelitic and psammitic schist; calc-silicate rock; minor amphibolite.|
75111|Leake Spring Metamorphics|72259|6|Mentioned|p3, p5-6|Orosirian|Orosirian|[Article examines the age and geochemistry of rutile from this unit].|ca. 1840-1810 Ma||||Includes pelitic gneisses.|
75111|Leake Spring Metamorphics|73102|5|Briefly described|p3, p20|||Gascoyne Province.||||Intruded by Kulkatharra Dolerite.|Pelitic and psammitic schist; calc-silicate rock; minor amphibolite.|
75111|Leake Spring Metamorphics|73168|6|Mentioned|p765|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|||||Volcano-sedimentary protoliths.|
75111|Leake Spring Metamorphics|73214|5|Briefly described|p974 Fig.1, 983|Palaeoproterozoic|Palaeoproterozoic|A xenotime age of 1817 +/- 17 Ma from a feldspathic metasandstone is of either xenotime growth during metamorphism or from a detrital grain.|1842-1807 Ma (protolith deposition).|||||
75111|Leake Spring Metamorphics|73442|5|Briefly described|p3|||Gascoyne Province.|||||Pelitic and psammitic schist; calc-silicate rock; minor amphibolite.|
80794|Leederville Supersequence|71958|2|Defined|p38, p40-p41, p45-p46|Aptian|Barremian|Vlaming Sub-basin. Sequence stratigraphy. Partially incorporates the Leederville Formation after which it is named. The type locality occurs in Warnbro 1 (-32.23769, 115.347327) between 1489 and 1081.6m (total thickness of 407.4m). Age is derived by the presence of diagnostic microfossils including B. Jaegeri, O. operculata, F.monilifera and D. davidii Dinocyst zones. Highly fossiliferous in places. The maximum thickness penetrated by a well is 499.7m at Warnbro 1. Offshore the sequence is thickest in the southern Vlaming Sub-basin over the Southern Peel Arch in the Bathurst Syncline. In the northern Vlaming Sub-basin this unit is thickest in the east. Interpreted to have been deposited in a shallow marine to fluvial environment. See also p51, p54, p60-p62, p64-p65.||Warnbro Megasequence||Conformably overlies the South Perth Supersequence. Unconformably overlain by the Coolyena Megasequence.|Fine to very coarse-grained sandstones containing glauconite, mica and minor feldspar interbedded with pyritic, glauconitic argillaceous and micaceous mudstones.|
32219|Leilira Formation|23416|5|Briefly described|Map Legend|Archean|Archean|Of Sulphur Springs Group. geological province:  Pilbara Craton.||||||07-NOV-08
32219|Leilira Formation|23755|4|Described|p36|Archean|Archean|See also page 17 table 1. Of Sulphur Springs Group.||||||16-APR-13
32219|Leilira Formation|23783|5|Briefly described|p16|Archean|Archean|Of Sulphur Springs Group.  Age: c.3255Ma.||||||07-NOV-08
32219|Leilira Formation|23891|5|Briefly described|p90|Archean|Archean|Of Sulphur Springs Group. Geological Province: Pilbara Craton.||||||07-NOV-08
32219|Leilira Formation|23956|5|Briefly described|p1264|||Of the Sulphur Springs Group. Geological Province: Pilbara Craton.||||||
32219|Leilira Formation|24025|4|Described|p8 Tb. 1|Archean|Archean|Of Sulphur Springs Group.  Wacke and intercalated rhyolite, sandstone, mudstone, chert.  Max. thickness: 3900Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
32219|Leilira Formation|24184|5|Briefly described|p702, p699 Fig.3|Archean|Archean|Of the Sulphur Springs Group. Overlain by: Kunagunarrina Formation. Geological Province: Pilbara Craton. Age: ca.3255Ma (SHRIMP U-Pb, Buick et al 2002)||||||07-NOV-08
32219|Leilira Formation|24531|4|Described|p19, p5 Tb. 1, p6|Archean|Archean|Now incorporates the former Six Mile Creek Formation. Of the Sulphur Springs Group (Pilbara Supergroup). Composed of interbedded fine- to medium-grained lithic arenite and wacke. Unconformably overlies the Warrawoona Group. Geol. Prov: Pilbara Craton.||||||16-APR-13
32219|Leilira Formation|24532|5|Briefly described|Map legend|Archean|Archean|Of the Sulphur Springs Group (Pilbara Supergroup).  Age: c.3240Ma.||||||07-NOV-08
32219|Leilira Formation|24550|5|Briefly described|p31 Tb. 3.1|Archean|Archean|Of the Sulphur Springs Group. Wacke, rhyolite, sandstone, mudstone, chert.||||||07-FEB-11
32219|Leilira Formation|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Of the Sulphur Springs Group. Wacke and intercalated rhyolite, sandstone, mudstone, chert.||||||07-FEB-11
32219|Leilira Formation|50379|5|Briefly described|Map Legend|Archean|Archean|Of Sulphur Springs Group (Pilbara Supergroup). Geological Province: Pilbara Craton.||||||07-NOV-08
32219|Leilira Formation|61253|5|Briefly described|p51|Archean|Archean|Basal unit of Sulphur Springs Group. Unconformably overlies the Kelly Group.  Geological Province: Pilbara Craton.||||||07-NOV-08
32219|Leilira Formation|61256|5|Briefly described|p340 Fig. 5a|Archean|Archean|Of the Sulphur Springs Group.  Sedimentary rocks. Overlies Euro Basalt; overlain by Kunagunarrina Formation.||||||07-NOV-08
32219|Leilira Formation|61266|4|Described|p58 Tb.1, p59|Archean|Archean|Of Sulphur Springs Gp. Conformably overlies Six Mile Creek Fm, unconformably overlies Warrawoona Gp in two places. Overlain by Kangaroo Caves Fm and conformably by Kunagunarrina Fm. Max. thickness: 3900. Geol. Prov: Pilbara Craton.||||||07-NOV-08
32219|Leilira Formation|61579|5|Briefly described|p58 Fig. 2|Archean|Archean|Of the Sulphur Springs Group. ||||||07-NOV-08
32219|Leilira Formation|63420|5|Briefly described|Map legend|Archean|Archean|Of Sulphur Springs Group (Pilbara Supergroup). Age: c.3255Ma. Geological Province: Pilbara Craton. Quartz sandstone, hydrothermal quartz(-biotite) cement; minor quartz carbonate layered rock and siltstone; metamoprhosed.||||||07-NOV-08
32219|Leilira Formation|63441|5|Briefly described|p4 Tb. 1|Archean|Archean|Of Sulphur Springs Group (pilbara Supergroup).||||||07-FEB-11
32219|Leilira Formation|63538|4|Described|p6 Fig. 3|Archean|Archean|Of Sulphur Springs Group. Overlain by Kunagunarinna Formation. Geological Province: Pilbara Craton. Sedimentary rocks.||||||19-APR-13
32219|Leilira Formation|64328|5|Briefly described|p56 Tb. 1|||Of Sulphur Springs Group.  Sandstone, felsic volcanic rocks.||||||07-FEB-11
32219|Leilira Formation|64405|5|Briefly described|p4 Fig. 3|Archean|Archean|Name inferred from Leilira only in Figure 3. Of the Sulphur Springs Group (De Grey Supergroup). Age: </-3273-3255Ma. Sedimentary.||||||07-FEB-11
32219|Leilira Formation|66745|3|Fully described|pp53-54, pp56-57.|Paleoarchean|Paleoarchean|Erosion and siliciclastic sedimentation, following a major event of vertical deformation (doming) and regional metamorphism (c.3290-3270 Ma).|c.3255 Ma.|Basal unit in Sulphur Springs Group.||Unconformably overlies Charteris Basalt. Is overlain by Kunagunarinna Formation.|Contains felsic volcanic and volcaniclastic components and wacke.|
32219|Leilira Formation|67130|5|Briefly described|p16|Paleoarchean|Paleoarchean||3270 - 3250 Ma|Sulphur Springs Group||Overlain by  Kunagunarrina Formation|Basal sandstone and felsic volcaniclastic rocks.|
32219|Leilira Formation|67197|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Sulphur Springs Group.||||
32219|Leilira Formation|67201|5|Briefly described|p7 Fig.4, p12 Tb.1|||In northern Pilbara Craton, East Pilbara Terrane.|< 3270 Ma|Sulphur Springs Group||||
32219|Leilira Formation|67269|5|Briefly described|p6 Fig.3|Paleoarchean|Paleoarchean||c.3255 Ma.|Sulphur Springs Group.||Unconformably overlies Euro Basalt or Charteris Basalt. Is overlain by Kunagunarinna Formation.|Siliciclastic rocks.|
32219|Leilira Formation|67270|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.|c.3255 Ma.|Sulphur Springs Group.||||
32219|Leilira Formation|67668|6|Mentioned|Fig. 2;||Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Sulphur Springs Group||Unconformably overlies the Charteris Basalt (Kelly Group), underlies the Kunagunarrina Formation.||
32219|Leilira Formation|68035|4|Described|p287,  p288 Fig 4|Paleoarchean|Paleoarchean|Pilbara Supergroup, East Pilbara Terrane, Pilbara Craton. Siliciclastic rocks up to 3.9 km thick. Occur at the base of the Sulphur Springs Group.|~3255 Ma|Of Sulphur Springs Group.||Unconformably overlies Charteris Basalt, Kelly Group. Overlain by Kunagunarinna Formation.|Siliciclastic rocks.|
32219|Leilira Formation|68280|5|Briefly described|p4||||c. 3255 Ma|Sulphur Springs Group||Unconformably overlies Charteris Basalt, overlain by Kunagunarinna Formation|Siliciclastic rocks.|
32219|Leilira Formation|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c. 3255 Ma (Buick et al. 2002).|Of the Sulphur Springs Group.|||Quartzite with hydrothermal quartz(-barite) cement; minor quartz-carbonate layered rock and metasiltstone.|
32219|Leilira Formation|68282|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c.3255 Ma (Buick et al. 2002).|Of the Sulphur Springs Group|||Silicified fine-grained felsic volcaniclastic rocks, layered grey, white, and cream chert; wacke, local volcaniclastic sandstone, shale, and quartzite, metamorphosed.|
32219|Leilira Formation|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c. 3255 Ma (Buick et al. 2002).|Of the Sulphur Springs Group.|||Quartz sandstone; hydrothermal quartz(-barite) cement; minor quartz-carbonate layered rock and siltstone; metamorphosed.|
32219|Leilira Formation|68284|5|Briefly described|p7|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Sulphur Springs Group.||Unconformably overlies Charteris Basalt (Kelly Group). Is overlain by Kunagunarinna Formation.||
32219|Leilira Formation|69013|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane. 3 facies are mapped separately.|c. 3255 Ma (Buick et al., 2002)|Of the Sulphur Springs Group.|||Wacke; local volcaniclastic sandstone, shale, and quartzite; metamorphosed. Dacite; includes local minor felsic schist; metamorphosed. Rhyolite and felsic volcaniclastic rocks; metamorphosed.|30-APR-14
32219|Leilira Formation|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Mapped as 4 unnamed sub-units.|c. 3255 Ma (Buick et al. 2002).|Of the Sulphur Springs Group.|||Silicified fine-grained felsic volcaniclastic rocks, layered grey, white and cream chert; chert; wacke, local volcaniclastic sandstone, shale, and quartzite, metamorphosed; dacite, includes local minor felsic schist, metamorphosed.|02-MAY-14
32219|Leilira Formation|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Dacite, rhyolite and felsic volcaniclastic rocks; metamorphosed.||Sulphur Springs Group|||Muscovite-bearing quartzite; metamorphosed sandstone, siltstone, chert, and mudstone. Quartzite interlayered with paragneiss. Silicified fine grained felsic volcaniclastic rocks, wacke, local volcaniclastic sandstone and shale; metamorphosed.|
32219|Leilira Formation|69301|4|Described|p5 Fig.3, p8, p9 Tb.1|||Pilbara Craton. East Pilbara Terrane. Thickness: up to 3.9 km.|3270 Ma|Sulphur Springs Group||Unconformable base.|Siliciclastic rocks.|
32219|Leilira Formation|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.|3255-3245 Ma (inferred)|Unit of Sulphur Springs Group.|||Chert, dacite, interlayered quartize and paragneiss, metamorphosed rhyolite and felsic volcaniclastics, layered chert, wacke; local volcaniclastic sandstone, shale and quartzite; metamorphosed.|
32219|Leilira Formation|69616|5|Briefly described|p161|Archean|Archean|||Unit in Sulphur Springs Group.||Is overlain by Kunagunarrina Formation.||
32219|Leilira Formation|70022|6|Mentioned|p115|||East Pilbara Terrane.||Sulphur Springs Group.||||
32219|Leilira Formation|70775|5|Briefly described|p12||Paleoarchean|East Pilbara.|< 3270 Ma|Sulphur Springs Group||Unconformably overlies the Charteris Basalt. Overlain by the Kunagunarinna Formation.||
32219|Leilira Formation|70884|5|Briefly described|p123|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Sulphur Springs Group.||Overlain by Kunagunarinna Formation. Underlain unconformably by Charteris Basalt/Kelly Group.||
32219|Leilira Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Sulphur Springs Large Igneous Province, East Pilbara Terrane.||Sulphur Springs Group|||Siliciclastic sedimentary rocks, minor felsic volcanic rocks, and chert; metamorphosed.|
32219|Leilira Formation|72064|5|Briefly described|p66|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Sulphur Springs Group.||Lowermost unit of Sulphur Springs Group. Overlain by Kunagunarinna Formation. Underlain unconformably by Charteris Basalt/Kelly Group.||
32219|Leilira Formation|72251|5|Briefly described|p54|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Sulphur Springs Group.||Lowermost unit of Sulphur Springs Group. Overlain by Kunagunarinna Formation. Underlain unconformably by Charteris Basalt.||
32219|Leilira Formation|72668|5|Briefly described|p4-6|||East Pilbara Terrane.|3270-3250 Ma|Sulphur Springs Group||Overlain by the Kunagunarinna Formation.|Basal sandstone and felsic volcaniclastic rocks.|
32219|Leilira Formation|73598|6|Mentioned|p1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Sulphur Springs Group.||Unconformably overlies Charteris Basalt. Is overlain by Kunagunarinna Formation.||
35642|Leinster Monzogranite|23281|6|Mentioned|p6|||||||||
35642|Leinster Monzogranite|71212|5|Briefly described|p86, p90, p248|||Yilgarn Craton. |||||Fine to medium-grained, largely massive, granite and monzogranite with strongly deformed margins.|
35642|Leinster Monzogranite|73151|6|Mentioned|p3-4|||Yilgarn Craton.|||||Granitic rocks.|
39661|Leo Member|24449|2|Defined|p751 App. 1|Llanvirnian|Llanvirnian|Of the Nita Formation.  Conformably overlain by Cudalgarra Member; conformably overlies Goldwyer Formation.  Geological Province: Canning Basin.  See also p743 Fig.5. Type seciton  in CRA Exploration P/L mineral exploration hole DD87SS7 from 1482.9 to 1545.5 m. Boundaries probably diachronus.||||||02-MAR-20
39661|Leo Member|64643|5|Briefly described|p3 Fig. 2|Darriwilian|Darriwilian|Of Nita Formation?||||||
39661|Leo Member|65449|4|Described|p5-6, p8, p47-48; Plates 1-11|Darriwilian|Darriwilian|Of McCracken (1994).||Of Nita Formation.||Overlies Goldwyer Formation. Is overlain by Cudalgarra Member.|An upward trend of increasing carbonate.|09-APR-20
39661|Leo Member|69883|4|Described|p5, p10, p12, p14|||Western Canning basin. The stratotype for this member is within DD87SS7. 27-80m thick. A reference section is interpreted in Leo 1 (1565-1642m). See also p27, p36, plate 1, plate 3.||Nita Formation||||02-MAR-20
81646|Leopold Downs Dyke Suite|71267|5|Briefly described|2_5m_interpdykel15_lut.csv|Proterozoic|Proterozoic|Events: Western Australian events (4000-0.01 Ma).|2500-541 Ma (inferred)||||Dolerite; mainly northeast-trending dykes|19-SEP-19
26273|Leschenault Formation|22742|4|Described|Table 3, Fig. 3, p119|Holocene|Holocene|Also p116. Age: 8280-5490 BP. Unconformably overlies Tamala Limestone. Unconformably overlain by Safety Bay Sand.||||||05-NOV-14
26273|Leschenault Formation|37480|6|Mentioned|p51|||||||||
26273|Leschenault Formation|40085|6|Mentioned|p203|||||||||
26273|Leschenault Formation|40314|4|Described|p203|||||||||
26273|Leschenault Formation|40367|2|Defined|p76|Holocene|Holocene|Overlies Eaton Sand gradationally; and Australind Fm where Eaton Sand and Tamala Lst. have eroded away; overlain by Safety Bay Sand. Thickness: up to 6m. Grey to dark grey sand (quartz skeletal and quartz) muddy sand and mud.||||||07-AUG-07
26273|Leschenault Formation|40400|6|Mentioned|p109|||Of Semeniuk (1983). Conformably overlain by bridport Calcilutite. Geological Province: Perth Basin.||||||06-AUG-07
26273|Leschenault Formation|40401|6|Mentioned|p122|||||||||
26273|Leschenault Formation|41200|5|Briefly described|p27|||Conformably overlain by Bridport Calcilutite. Bioturbated.||||||06-AUG-07
26273|Leschenault Formation|41502|4|Described|Table 1|||||||||
26273|Leschenault Formation|41504|6|Mentioned|p71|||||||||
26273|Leschenault Formation|42076|5|Briefly described|p3|||||||||
26273|Leschenault Formation|63454|5|Briefly described|p71 Tb. 3|||Grey sand, mud, muddy sand, locally shelly; estuarine shells.||||||
25993|Lesueur Sandstone|12758|4|Described|p15, p3 Fg. 3early trias|Late Triassic|Early Triassic|Overlain by Cattamarra C.M; conformably overlies Sabina Sst. in South Perth Basin; overlies Woodada Formation transitionally in North Perth Basin.  Overlain by Cattamarra C.M. in SPB and Eneabba Fm. in central part of Perth Basin.  See also p8 Fig. 9.||||||
25993|Lesueur Sandstone|14227|5|Briefly described|p8, p10|Late Triassic|Middle Triassic|Includes Wonnerup Member. Appears to be transitional, after Woodada Formation, into Eneabba Formation above. Thick and distinctive unit of almalgamated fluvial sands. See also Enclosure 2. Geol. Prov: Bunbury Trough, southern Perth Basin.||||||07-FEB-11
25993|Lesueur Sandstone|14228|6|Mentioned|p5 fig 2, p8|Late Triassic|Late Triassic|||||Overlain by Eneabba Formation. Overlies Woodada Formation.||
25993|Lesueur Sandstone|22814|5|Briefly described|fig2|Triassic|Triassic|||||||
25993|Lesueur Sandstone|23172|4|Described|Map Legend|Triassic|Triassic|||||||
25993|Lesueur Sandstone|23279|4|Described|p20,23-5|Hettangian|Anisian|||||||
25993|Lesueur Sandstone|23520|5|Briefly described|p6 Fig. 4|Late Triassic|Middle Triassic|Geological Province: Abrolhos Sub-basin.  See also p9.||||||
25993|Lesueur Sandstone|23816|4|Described|p239|Early Triassic|Early Triassic|Geological Province: Perth Basin. Underlying unit: Woodada Formation (disconformable). Overlying unit: Cockleshell Gully Formation (conformable). Max. thickness: >2201 m.||||||
25993|Lesueur Sandstone|24058|5|Briefly described|p112|Late Triassic|Late Triassic|Poorly sorted coarse kaoloinitic sandstone and conglomerates with rare interbeds of siltstone.  Max. thickness: 2130m.||||||
25993|Lesueur Sandstone|24390|5|Briefly described|p15 Fig. 8|Triassic|Triassic|Geological Province: Perth Basin.||||||
25993|Lesueur Sandstone|24410|5|Briefly described|p41|Triassic|Triassic|Widely distributed in the subsurface north of Dongara. Consists mostly of fine- to very coarse-grained cross-bedded quartz sandstone. Geological Province: northern Perth Basin.||||||24-NOV-09
25993|Lesueur Sandstone|24443|5|Briefly described|Fig.30, 31|Late Triassic|Middle Triassic|Overlies Woodada Formation and Sabina Sandstone (conformable). Overlain by Eneabba Formation and Cattamarra Coal Measures. Geological Province: Bight Basin.||||||
25993|Lesueur Sandstone|29693|6|Mentioned|Fig.7|||||||||
25993|Lesueur Sandstone|29721|6|Mentioned|Table 226|||||||||
25993|Lesueur Sandstone|30565|6|Mentioned|p135|||||||||
25993|Lesueur Sandstone|30963|6|Mentioned|Map legend|Late Triassic|Late Triassic|||||||
25993|Lesueur Sandstone|31237|6|Mentioned|p21|||||||||
25993|Lesueur Sandstone|31238|5|Briefly described|p28|||||||||
25993|Lesueur Sandstone|31562|6|Mentioned|p10|||Stratigraphic Table.||||||
25993|Lesueur Sandstone|31568|5|Briefly described|p18|||U. Triassic See also Fig. 2||||||
25993|Lesueur Sandstone|31910|3|Fully described|Table 1|||P.20||||||
25993|Lesueur Sandstone|32165|6|Mentioned|p196|||Sections BMR10 & 10A correlated||||||
25993|Lesueur Sandstone|32648|6|Mentioned|p32|||Triassic||||||
25993|Lesueur Sandstone|32650|6|Mentioned|p89|||||||||
25993|Lesueur Sandstone|32714|6|Mentioned|Fig.2|||||||||
25993|Lesueur Sandstone|33386|6|Mentioned|Fig.7|||||||||
25993|Lesueur Sandstone|34008|2|Defined|p75|Triassic|Triassic|See also pp71,73,76||||||08-OCT-20
25993|Lesueur Sandstone|34010|6|Mentioned|Cor. chart|||M - U Triassic||||||
25993|Lesueur Sandstone|34841|6|Mentioned|Fig.2|||||||||
25993|Lesueur Sandstone|35282|6|Mentioned|p31|||See also Fig.2||||||
25993|Lesueur Sandstone|35573|6|Mentioned|Fig.13|||Generalised stratigraphy - Perth Basin||||||
25993|Lesueur Sandstone|35653|6|Mentioned|p1093|||Discussion of stratigraphy and basin development. See also Fig.3.||||||
25993|Lesueur Sandstone|35968|5|Briefly described|p63|||Hydrogeology P65.||||||
25993|Lesueur Sandstone|36100|6|Mentioned|Fig.2|||||||||
25993|Lesueur Sandstone|36257|6|Mentioned|Table 2.1|||||||||
25993|Lesueur Sandstone|36265|5|Briefly described|Fig.3.26|Late Triassic|Late Triassic|Geological province: Perth Basin.||||||04-MAR-08
25993|Lesueur Sandstone|36293|2|Defined|p130|Triassic|Triassic|||||||
25993|Lesueur Sandstone|36890|3|Fully described|p239|||||||||
25993|Lesueur Sandstone|36911|6|Mentioned|p58|||||||||
25993|Lesueur Sandstone|37104|6|Mentioned|Fig.3|||||||||
25993|Lesueur Sandstone|38221|6|Mentioned|Fig.4|||Perth Basin||||||
25993|Lesueur Sandstone|38777|5|Briefly described|p29|||||||||
25993|Lesueur Sandstone|39155|5|Briefly described|p18|||Aquifer characteristics||||||
25993|Lesueur Sandstone|40358|6|Mentioned|p22|||||||||
25993|Lesueur Sandstone|40359|5|Briefly described|p22|||||||||
25993|Lesueur Sandstone|40992|6|Mentioned|Fig.5|||||||||
25993|Lesueur Sandstone|41172|4|Described|p126|||||||||
25993|Lesueur Sandstone|41192|6|Mentioned|Fig.5|||||||||
25993|Lesueur Sandstone|41195|6|Mentioned|Fig.2|||||||||
25993|Lesueur Sandstone|41284|4|Described|p90|||||||||
25993|Lesueur Sandstone|41728|6|Mentioned|p441|||||||||
25993|Lesueur Sandstone|41729|5|Briefly described|p454|||||||||
25993|Lesueur Sandstone|41782|6|Mentioned|p26|||||||||
25993|Lesueur Sandstone|41989|6|Mentioned|Fig.3 P110|||||||||
25993|Lesueur Sandstone|42075|5|Briefly described|Fig.7 P247|||||||||
25993|Lesueur Sandstone|42434|6|Mentioned|p5|||||||||
25993|Lesueur Sandstone|42687|6|Mentioned|map legend|Triassic||||||||
25993|Lesueur Sandstone|42688|6|Mentioned|map legend|Triassic||||||||
25993|Lesueur Sandstone|42734|5|Briefly described|map legend|Triassic||||||||
25993|Lesueur Sandstone|43031|4|Described|p15,Fig.2|||||||||
25993|Lesueur Sandstone|43062|5|Briefly described|p19,Table 2,p18|||||||||
25993|Lesueur Sandstone|43067|6|Mentioned|Fig.7,p119|||||||||
25993|Lesueur Sandstone|43096|4|Described|p5|||see also Fig.2||||||
25993|Lesueur Sandstone|43197|5|Briefly described|Map Legend||Triassic|||||||
25993|Lesueur Sandstone|43212|6|Mentioned|p5||Triassic|||||||
25993|Lesueur Sandstone|43216|5|Briefly described|Map Legend||Triassic|Perth Basin||||||
25993|Lesueur Sandstone|43217|5|Briefly described|Map Legend||Triassic|Perth Basin||||||
25993|Lesueur Sandstone|43296|5|Briefly described|Map Legend||Triassic|||||||
25993|Lesueur Sandstone|43297|4|Described|p10,Fig.3 p5.|Norian|Anisian|see also Table 1 p6.Type,section location given. Middle to Late Triassic.||||||
25993|Lesueur Sandstone|43347|4|Described|5|Early Jurassic|Middle Triassic|||||||
25993|Lesueur Sandstone|43495|4|Described|6-36|Norian||||||||
25993|Lesueur Sandstone|43504|4|Described|4-10|Norian|Anisian|||||||
25993|Lesueur Sandstone|43705|6|Mentioned|p11||Triassic|||||||
25993|Lesueur Sandstone|44144|4|Described|p506 Tb. 4-21, p509 Fig.4-145, p513-514|Late Triassic|Early Triassic|Type Section: Woolmulla 1; 429-1012m. Over 2200m thick fluvial deposits. Thins westwards; deposited as a series of fans along a fault scarp.||||Overlies Woodada Formation or Sabina Sandstone (both conformably). Overlain conformably by Cockleshell Gully Formation.|Light grey, fine- to very coarse-grained, cross-bedded quartz sandstone; minor siltstone.|
25993|Lesueur Sandstone|44307|2|Defined|p11-16||Triassic|U/lies Cockleshell Gully Fm.; O/lies Woodada Fm. Middle-Upper Triassic. (H50-5,9).||||||
25993|Lesueur Sandstone|45168|6|Mentioned|Table 1|||||||||
25993|Lesueur Sandstone|48614|4|Described|p5,29,31,34,46|||(New name). (H50-5,9). See also Pl. 1,5,6,8,9.||||||
25993|Lesueur Sandstone|49942|4|Described|p4 Fig.3|Late Triassic|Middle Triassic|Conformably overlies Woodada Formation. Conformably overlain by Eneabba Formation. Geological Province: Gascoyne Platform.||||||
25993|Lesueur Sandstone|50085|5|Briefly described|p15 Fig. 8|Triassic|Triassic|Geological Province: Northern Perth Basin.||||||11-MAY-04
25993|Lesueur Sandstone|50107|5|Briefly described|Map legend|Triassic|Triassic|Geological Province: Southern and Northern Perth Basin.||||||
25993|Lesueur Sandstone|60376|5|Briefly described|p17 Fig. 4.|Late Triassic|Early Triassic|Geological Province: Perth Basin. Overlain unconformably by Eneabba Formation. Underlain by Woodada Formation, Arranoo Sandstone, Kockatea Shale and Sabina Sandstone.||||||07-FEB-11
25993|Lesueur Sandstone|60377|5|Briefly described|p61 Fig. 3|Rhaetian|Anisain|Underlain by Woodada Formation. Geological Province: Perth Basin. Fluvial depositional environment.||||||07-FEB-11
25993|Lesueur Sandstone|60384|6|Mentioned|p244, p243 Fig 2a|Late Triassic|Middle Triassic|Perth Basin.||||||
25993|Lesueur Sandstone|61023|5|Briefly described|p20 Fig 10|Triassic|Triassic|Geological Province: Perth Basin.||||||11-APR-08
25993|Lesueur Sandstone|61546|6|Mentioned|p383, p385 Fig.5. |Triassic|Triassic|Regressive continental deposition.||||Overlies Woodada Formation. Is overlain by Eneabba Member.||
25993|Lesueur Sandstone|61811|5|Briefly described|p3 Fig.2, p49, p64.|Rhaetian|Anisian|Northern Perth Basin. Type section details in Appendix 1.||||Overlies Woodada Formation. Is overlain by Eneabba Formation.|Festoon cross-bedded sandstone.|
25993|Lesueur Sandstone|63929|6|Mentioned|p131 Fig.2.|Late Triassic|Early Triassic|Perth Basin. Predominantly non-marine clastic sediments.||||Overlies Woodada Formation.||
25993|Lesueur Sandstone|64580|4|Described|map legend|Late Triassic|Early Triassic|Very fine- to very coarse-grained quartz sandstone; subordinate granule conglomerate; minor siltstone.||||||09-DEC-08
25993|Lesueur Sandstone|64635|5|Briefly described|p4 Fig.3 |Rhaetian|Anisian|||||Overlies Woodada Formation. Is overlain by Eneabba Formation.||
25993|Lesueur Sandstone|66124|4|Described|p169, p170 Fig.2|Rhaetian|Olenekian|Perth Basin. Overlies Woodada Formation. Non-marine, probably fluvial. Coarse-grained sandstone, minor siltstone and conglomerate. 1100 to 3000m thick.||||||
25993|Lesueur Sandstone|67135|5|Briefly described|p5 Fig.7, p72.|Triassic|Triassic|Perth Basin. A saline aquifer with potential for CO2 storage.||||Overlies Woodada Formation. Is overlain by Eneabba Formation.||
25993|Lesueur Sandstone|67340|6|Mentioned|p6-8, 19, 25, 50-62|Triassic|Triassic|Northern Perth Basin. Thermal rock properties. Wells in this unit used for this Report are listed.||||||
25993|Lesueur Sandstone|67888|6|Mentioned|p82|||||||||
25993|Lesueur Sandstone|67925|5|Briefly described|Ch2 p10 fig 4, Ch2 p11|Rhaetian|Scythian|See also Ch2 p44-p45, Ch3 p8, Ch4 p8 fig 2, Ch4 p30 fig 34, Ch5 p26, Ch8 p11.|||Includes the Wonnerup Member and the Myalup Member.|Overlies the Sabina Sandstone and the Woodada Formation. Overlain by the Cockleshell Gully Formation, Eneabba Formation and the Cattamarra Coal Measures.||
25993|Lesueur Sandstone|69029|5|Briefly described|p332|Rhaettian|Ladinian|Of Perth Basin.|||Includes Myalup and Wonnerup members.|Overlain by Enneabba Formation. Underlain by Woodada Formation.||
25993|Lesueur Sandstone|69081|5|Briefly described|p736,p740-1, Figs.3-4,  Tbs.1-3|||Presented as Lesueur Sst in figure, and Lesueur in table. Potential target for CO2 geosequestration project. Geol. Prov: Perth Basin.|||Yalgorup Member, Wonnerup Member|Is overlain by Cattamarra Coal Measures and Eneabba Formation; overlies Sabina Sandstone.|Medium to very coarse-grained sandstone.|23-JUL-15
25993|Lesueur Sandstone|69182|4|Described|p3, p7, p13, Ch2 p3, Ch2 p9|Early Triassic|Early Triassic|Perth Basin. One of the best potential reservoirs in the Perth Basin for the storage of CO2 as it has good reservoir properties and is sealed by the Eneabba Formation. Deposited as part of a fluvial system. See also Ch2 p13, Ch2 p20-p29, Ch2 p34-p42, Ch2 p44, Ch2 p46, Ch2 p50-p51, Ch2 p55, Ch2 p57, Ch2 p60-p64, Ch2 p67, Ch2 p69, Ch2 p72-p74, Ch2 p79, Ch2 p83-p90, Ch2 p93-p102, Ch2 p105, Ch2 p107, Ch2 p109, Ch2 p110, Ch2 p112, Ch3 p12.|||Includes the Wonnerup Member and the Myalup Member.|Overlies the Sabina Sandstone, Kockatea Shale and the Woodada Formation. Overlain by the Eneabba Formation and the Cattamara Coal Measures.|Medium to coarse-grained, Quartzo-feldspathic sandstone interbedded with shale and siltstone.|
25993|Lesueur Sandstone|69297|6|Mentioned|p175, p189, p202|Norian|Olenekian|Vlaming Sub-basin, South Perth Basin. ||||Overlies the Sabina Sandstone. Overlain by the Eneabba Sequence.||
25993|Lesueur Sandstone|70097|5|Briefly described|p2, p19-22 Figs.3-6|Toarcian|Anisian|Regression; deltaic and fluvial facies of Woodada Formation and Lesueur Sandstone. Perth Basin. Greenough/Bookara Shelf, Dongara Saddle, Dandaragan Trough, Beermullah Trough and Mandurah Terrace.|||Myalup Member, Wonnerup Member|Overlies Sabina Sandstone or Woodada Formation. Is overlain by Cattamarra Coal Measures or Eneabba Formation.|Sandstone.|12-SEP-17
25993|Lesueur Sandstone|70099|5|Briefly described|Fig.4; p5|Rhaetian|Olenekian|Southern Perth Basin. Correlated to seismic package Mentelle 1B, with Sabina Sandstone and Willespie Formation.||||Overlies Sabina Sandstone. Is overlain by Cattamarra Coal Measures.||
25993|Lesueur Sandstone|70128|5|Briefly described|p449, p451, p454-455, p457, p459-465|Late Triassic|Late Triassic|Perth Basin. Modelled thickness distribution histogram.||||Conformably overlies Woodada Formation and Sabina Sandstone. Is overlain conformably by Cattamarra Coal Measures and unconformably by Eneabba Formation.|Predominantly sand-rich and oxidised; unfavourable for high-resolution palaeontological dating.|
25993|Lesueur Sandstone|70796|5|Briefly described|500k_interpgeop14_lut.csv|Upper Triassic|Lower Triassic|Perth Basin. Formed during Gondwana breakup along the western margin.|252.17  201.3 Ma (biostrat)||||Very fine to very coarse grained quartz sandstone; subordinate granule conglomerate; minor siltstone.|
25993|Lesueur Sandstone|70826|6|Mentioned|p7 tbl 4|Triassic|Triassic|Perth Basin.||||||
25993|Lesueur Sandstone|71146|5|Briefly described|p6|Middle Triassic|Early Triassic|Perth Basin.||||Overlies the Sabina Sandstone and the Woodada Formation.|Sandstone.|
25993|Lesueur Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
25993|Lesueur Sandstone|71269|5|Briefly described|500k_interpgeop16_lut.csv|Late Triassic|Middle Triassic|Of Perth Basin. Events: Mid-Miocene transgression, 15 Ma (15-15 Ma); Wilson Bluff transgression, 42 Ma (42-42 Ma); Kings Park transgression, 56 Ma (56-56 Ma); Gondwana breakup-western margin (210-125 Ma); Jurassic-Early Cretaceous rifting, Perth Basin (168-133 Ma);??|247.2-20.13 Ma (biostrat; inferred)||||Very fine to very coarse grained quartz sandstone; subordinate granule conglomerate; minor siltstone|
25993|Lesueur Sandstone|71377|4|Described|p1-p3, p7, p17, p41|Late Triassic|Middle Triassic|Perth Basin. SHRIMP ages are interpreted as the maximum depositional ages derived from detrital zircons in this study. Three additional ages are provided, these are: 527 +/- 9 Ma, 513 +/- 24 Ma and 513 +/- 14 Ma. These dates are considerably older than the biostratigraphic age of the Late Triassic. Intersected in GSWA Harvey 1 (700-2895m). Zircon morphology and sample descriptions are provided. See also p43-p47, p50, p52-p54, p59, p61-p63, p67, p69-p71, p85-p88, p90, p102-p104.|517 +/- 14 Ma (SHRIMP U-Pb)||Includes the Yalgorup Member and Wonnerup Member.|Conformably overlain by the Eneabba Formation.||
25993|Lesueur Sandstone|71958|5|Briefly described|p34|Triassic|Triassic|Vlaming Sub-basin.|||Includes the Wonnerup Member and the Myalup Member.|Overlies the Sabina Sandstone. Overlain by the Cattamarra Coal Measures and Eneabba Formation.||
25993|Lesueur Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Late Triassic|Middle Triassic|Perth Basin.  Max age from biostratigraphy, min age inferred.|||||Very fine to very coarse grained quartz sandstone; subordinate granule conglomerate; minor siltstone.|
25993|Lesueur Sandstone|72258|5|Briefly described|p129,133|Late Triassic|Middle Triassic|Of Perth Basin. Major peak in Mesoproterozoic (1300-1100 Ma) detrital zircons correlate with characteristic ages and Hf isotopic signatures of magmatism in the Albany-Fraser-Wilkes Orogen (Clark et al., 2000; Fitzsimons, 2000, 2003; Kirkland et al., 2011; Spaggiari et al., 2015). Late Meso- to Early Neoproterozoic (1100-900 Ma) detrital zircons atributed to Pinjarra Orogen. Neoproterozoic 600-500 Ma peak in detrital zircon ages also likely to be derived locally from Pinjarra Orogen (p134-135 describes potential, but unlikely Gondwanan sources).||||Overlain by Cattamarra Coal Meausres or Eneabba Formation. Underlain by, and laterally grades northward into Woodada Formation. Also underlain by Sabina Sandstone.||
25993|Lesueur Sandstone|73424|6|Mentioned|p5|Triassic|Triassic|Perth Basin.||||||
79247|Lesueur Sequence|69297|6|Mentioned|p204, p209, p223, p225, p236, p237, p238|||Perth Basin. ||||Overlies the Woodada Sequence. Overlain by the Eneabba Sequence.||
79247|Lesueur Sequence|70097|5|Briefly described|p3, p4|Late Triassic|Early Triassic|Subsidence, offshore northern Perth Basin. Fluvio-deltaic systems.||||||20-OCT-15
77866|Leviathan Suite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2696 Ma (inferred).||Includes Defiance, Eureka, Federal, Pernatty, Williamstown Dolerites; Mount Herbert, Powder, Yilmia Gabbros.|||
77866|Leviathan Suite|71270|5|Briefly described|100k_interpgeop_lut.csv|||Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton.|||Includes Defiance Dolerite, Eureka Dolerite, Federal Dolerite, Mount Herbert Gabbro, Pernatty Dolerite, Powder Gabbro, Mount Herbert Gabbro, Williamstown Dolerite, Yilmia Gabbro.|||
27821|Liberty Granodiorite|22534|4|Described|p12|||Age of unit 2593+/-10 Ma||||||
27821|Liberty Granodiorite|22539|5|Briefly described|Map legend|Archean|Archean|||||||07-NOV-08
27821|Liberty Granodiorite|22645|6|Mentioned|Table2 P209||Archean|Age of unit is 2648+/-6 Ma||||||07-NOV-08
27821|Liberty Granodiorite|23926|5|Briefly described|p22|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
27821|Liberty Granodiorite|24305|5|Briefly described|p928|||||||||
27821|Liberty Granodiorite|41786|4|Described|p333|||||||||
27821|Liberty Granodiorite|42156|6|Mentioned|p373|||Also called Lady Bountiful granite||||||
27821|Liberty Granodiorite|42221|6|Mentioned|p30|||||||||
27821|Liberty Granodiorite|42696|6|Mentioned|Plate 1B|Archean||||||||07-NOV-08
27821|Liberty Granodiorite|42870|6|Mentioned|p81|||||||||
27821|Liberty Granodiorite|43052|5|Briefly described|Fig.3.8|||||||||
27821|Liberty Granodiorite|43102|5|Briefly described|p4|||Age of 2593+/-10 Ma.||||||
27821|Liberty Granodiorite|43214|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
27821|Liberty Granodiorite|43232|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
27821|Liberty Granodiorite|43496|6|Mentioned|15|||Age: 2645+/-17Ma, 2675+/-23Ma||||||
27821|Liberty Granodiorite|60076|5|Briefly described|p45 App. 1|||[Agglb]   Fine- to coarse-grained; locally monzogranitic; massive.||||||
27821|Liberty Granodiorite|61849|5|Briefly described|p312, p313|Archean|Archean|Small tear-shaped post-tectonic Archaean pluton.  Quartz veins are common. weathering has produced a thick zone of saprolite comprising white, poorly indurated, matrix-supported medium quartz sandy clay.||||||06-AUG-15
27821|Liberty Granodiorite|64633|6|Mentioned|p14 Fig.9.|||Syn-extensional upper plate intrusion.||||||
27821|Liberty Granodiorite|65204|6|Mentioned|p18, p19 Tbl.4, p24|Neoarchean||~2650 Ma; 0.5-5mm grains; equigranular; hosts the Lady Bountiful gold deposit.||||||
27821|Liberty Granodiorite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Fine- to coarse-grained granodiorite; local monzogranite; massive; contacts discordant with greenstones and early foliation.||||||07-FEB-11
27821|Liberty Granodiorite|65834|6|Mentioned|p37-38, 40, 43-44|||Mount Pleasant district, Ora Banda Domain, Kalgoorlie Terrane. Hosts gold deposits (eg Lady Bountiful mine), described. Intrudes the gold-bearing sequence of units in the Mount Pleasant district. Described in some detail.|||||Late-tectonic, I-type granite. Contains enclaves comprising (a) Mount Pleasant Sill xenoliths, and (b) cognate microgranitoid enclaves.|
27821|Liberty Granodiorite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Fine- to coarse-grained granodiorite; local monzogranite; massive; contacts discordant with greenstones and early foliation.|06-AUG-15
27821|Liberty Granodiorite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Fine- to coarse-grained granodiorite; local monzogranite; massive; contacts discordant with greenstones and early foliation.|
27821|Liberty Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite|
27821|Liberty Granodiorite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|3010-2600 Ma (inferred)||||Fine- to coarse-grained granodiorite; local monzogranite; massive; contacts discordant with greenstones and early foliation|
27821|Liberty Granodiorite|73391|5|Briefly described|p22, 51, 242, 291, 295, 298, 304, 319|||See also p326, 329-332, 351, 422, Appendices. Owen Batholith, Kalgoorlie district. Intrudes the nose of the Mount Pleasant Anticline. Intrusion was synchronous with or late within the regional folding phase of deformation.|2648 +/- 6 Ma (SHRIMP: Kent, 1994).|||Intrudes Lower Basalt, Mount Pleasant Sill and Siberia Komatiite.|A small granitoid stock in the hinge of the Mount Pleasant Anticline.|
29411|Ligertwood beds|42940|5|Briefly described|Plate 2|Carboniferous|Carboniferous|Breccia, conglomerate, conglomeratic sandstone, sandstone.  Age: 360-290Ma. Geological province: Amadeus Basin.||||||23-JAN-08
29411|Ligertwood beds|61387|5|Briefly described|Map legend|Permian|Carboniferous|Breccia, sandstone, conglomerate, conglomeratic sandstone.||||||
29411|Ligertwood beds|61519|5|Briefly described|Map Legend|Permian|Carboniferous|Breccia, sandstone, conglomerate, conglomeratic sandstone.||||||
29411|Ligertwood beds|64778|6|Mentioned|p13|||Amadeus Basin.||||||
29411|Ligertwood beds|67856|4|Described|p347 tab 4-9, p337, p346, 348|Permian|Permian|Of Wells et al., 1964, 1970. Type section: Ligertwood Cliffs. About 25m thick. Correlated with Paterson Formation. Fluvio-glacial sequence. No age determination. Age assumed from correlation.||||Correlated with Crown Point Formation, Paterson Formation and in part with Grant Group.|Bedded dolomite/limestone conglomerate with secondary matrix of travertine followed by conglomerate and sandstone.|
29411|Ligertwood beds|69438|3|Fully described|p23:4, 42|Permian|Carboniferous|Wells et al. (1965); named after Ligertwood Cliffs, far NW Amadeus Basin, which form the type area. Exposed over a strike length of c.115km. Not folded; deposition post-dated the 450-300 Ma Alice Springs Orogeny.||||Corrlated (tentatively) with the Buck Formation in WA.|A lower interval of interbedded sandstone, calcareous sandstone and calcareous pebble and cobble conglomerate; disconformably overlain by an upper unit of interbedded silicified sandstone, conglomeratic sandstone, and pebble conglomerate.|12-JUL-16
29411|Ligertwood beds|70839|6|Mentioned|p330|Late Paleozoic|Late Paleozoic|||||||
29411|Ligertwood beds|71088|5|Briefly described|p12, p17, p33|Paleozoic|Paleozoic|Amadeus Basin. Units previously mapped as this formation have been reassigned to the new Mu Formation. The type area was on Mount Rennie in the NT.||||||
29411|Ligertwood beds|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sedimentary breccia, conglomerate, sandstone|
29411|Ligertwood beds|72360|5|Briefly described|Map legend|Permian|Carboniferous|Of Canning Basin.|||||Breccia, sandstone, conglomerate, conglomeratic sandstone.|09-SEP-19
78514|Lightfoot Orthogneiss|68107|5|Briefly described|p609 Tb.1, p612, p617.|Neoarchean|Neoarchean|Appears as Lightfoot orthogneiss in Table 1.|Protolith: 2738 +/- 3 Ma (Wingate et al. 2011b).||||Metagranodiorite.|
25994|Lightjack Formation|7433|4|Described|p25 Fig.2, p32 Fig.8, pp37-38, pp52-53.|Permian|Permian|Canning Basin. Lithology resembles Triwhite Sandstone. Coarse units contain labile detritus probably from Grant Group. Trace fossils very common. Marker beds: an Fe,Mn-enriched concretionary unit and a medium-grained quartz sandstone.||Basal unit of Liveringa Group.||Overlies Noonkanbah Formation. Is overlain by Condren Sandstone.|Planar thin- to medium-bedded micaceous siltstones; planar to lenticular, megarippled and cross-bedded, coarse quartzose sandstones. Local phosphatic, ochreous ironstones; oolitic ironstones. Has two marker beds.|
25994|Lightjack Formation|22741|5|Briefly described|P28, Table3 P12|Kungurian|Artinskian|||||||
25994|Lightjack Formation|22764|4|Described|Table2,p9|Late Permian|Early Permian|450 m. Conformable on Nookanbah Formation.||||||01-FEB-10
25994|Lightjack Formation|22767|5|Briefly described|Table3 P14, P22|Late Permian|Early Permian|||||||
25994|Lightjack Formation|22776|4|Described|Table.3|Kungurian|Artinskian|see also p19.||||||
25994|Lightjack Formation|23766|5|Briefly described|p20|Permian|Permian|Parent: Liveringa Group||||||
25994|Lightjack Formation|24466|5|Briefly described|p372|||||||||
25994|Lightjack Formation|29806|6|Mentioned|Map legend|Permian|Permian|||||||
25994|Lightjack Formation|29807|4|Described|Table 1|||||||||
25994|Lightjack Formation|29813|6|Mentioned|p7|||||||||
25994|Lightjack Formation|29817|4|Described|p8|||||||||
25994|Lightjack Formation|29818|6|Mentioned|Map legend|Permian|Permian|||||||
25994|Lightjack Formation|29819|6|Mentioned|Map legend|Permian|Permian|||||||
25994|Lightjack Formation|30342|6|Mentioned|Table 20|||||||||
25994|Lightjack Formation|33518|4|Described|Table 1|||||||||
25994|Lightjack Formation|33519|6|Mentioned|Map legend|Permian|Permian|||||||
25994|Lightjack Formation|33960|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
25994|Lightjack Formation|33962|6|Mentioned|Table 20|||||||||
25994|Lightjack Formation|33965|4|Described|Table 1|||||||||
25994|Lightjack Formation|33966|6|Mentioned|Map legend|Late Permian|Early Permian|Lower - Upper? Perm.||||||
25994|Lightjack Formation|35120|6|Mentioned|Map legend|Late Permian|Early Permian|Early - Late Permian Prob.||||||05-JUN-15
25994|Lightjack Formation|35124|6|Mentioned|Map legend|Late Permian|Early Permian|Early - Late Permian||||||
25994|Lightjack Formation|35205|6|Mentioned|Map legend|Permian|Permian|||||||
25994|Lightjack Formation|35222|6|Mentioned|p13|||||||||
25994|Lightjack Formation|35225|6|Mentioned|p9|||||||||
25994|Lightjack Formation|36224|5|Briefly described|Map legend|Late Permian|Early Permian|Of the Liveringa Group.  Mudstone, fine sandstone interbedded; clay pellet conglomerate; medium sandstone; plant fossils.||||||01-FEB-05
25994|Lightjack Formation|36225|6|Mentioned|Map legend|Late Permian|Early Permian|Early to Late Permian||||||
25994|Lightjack Formation|36634|6|Mentioned|Map legend|Late Permian|Early Permian|Early to Late Permian||||||
25994|Lightjack Formation|37549|6|Mentioned|Fig.10|||||||||
25994|Lightjack Formation|38878|6|Mentioned|Map legend|Tatarian|Kazanian|Kungurian - Tatarian||||||
25994|Lightjack Formation|40794|5|Briefly described|Fig.3|||||||||
25994|Lightjack Formation|41044|6|Mentioned|p156|||Probably Noonkanbah Formation||||||
25994|Lightjack Formation|41100|6|Mentioned|p280|||||||||
25994|Lightjack Formation|41158|6|Mentioned|p162|||||||||
25994|Lightjack Formation|41474|6|Mentioned|p59|||||||||
25994|Lightjack Formation|41688|6|Mentioned|p10|||||||||
25994|Lightjack Formation|41809|6|Mentioned|p65|||||||||
25994|Lightjack Formation|42994|6|Mentioned|p52|||||||||
25994|Lightjack Formation|43015|5|Briefly described|Table 1,p319|||||||||
25994|Lightjack Formation|43018|5|Briefly described|Table 1,p386|||||||||
25994|Lightjack Formation|43173|6|Mentioned|54||Early Permian|||||||
25994|Lightjack Formation|43563|6|Mentioned|Fig.2,p5||Kungurian|||||||
25994|Lightjack Formation|43932|4|Described|p8,Tb.1 p6||Permian|||||||
25994|Lightjack Formation|44143|4|Described|p.435 Table 4-19; p.446, Figure 4-102|Permian|Permian|Unit in Liveringa Group. Up to 300m thick; mudstone, sandstone, and conglomerate; shallow marine to lagoonal. Conformably overlies Noonkanbah Formation; is overlain conformably by Condren Sandstone; partly equivalent to Triwhite Sandstone. Type section at Lightjack Hill (NOONKANBAH: 18deg 59' S, 125deg 50' E). Contains bivalves, brachiopods, trace fossils and plant fragments: Atomodesma exerta and Stutchburia muderongensis are characteristic: late Artinskian to early Kazanian.||||||23-NOV-17
25994|Lightjack Formation|44231|5|Briefly described|Map Legend|Permian|Permian|Of the Liveringa Group. Fine-grained quartz wacke, ferruginous siltstone, and sandstone; shallow marine deltaic. Geological Province: Canning Basin.||||||26-MAY-05
25994|Lightjack Formation|44356|14|Not recorded|p9,Tb.1 p6|||||||||
25994|Lightjack Formation|45140|5|Briefly described|p51, p67|Permian|Permian|Canning Basin. Marine sediments.||Liveringa Group.||Overlaps Hidden Basin Beds. Conformably overlies Noonkanbah Formation. Is overlain conformably by Condren Sandstone.|Fossiliferous siltstone, sandstone and shale.|
25994|Lightjack Formation|45149|6|Mentioned|p49|||||||||
25994|Lightjack Formation|45153|2|Defined|App.4-73|Early Permian|Early Permian|Previously known as Lightjack Member and Balgo Member.||||||
25994|Lightjack Formation|45158|3|Fully described|p20|||See also p36||||||26-MAY-05
25994|Lightjack Formation|46849|6|Mentioned|Fig. 5|||||||||
25994|Lightjack Formation|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
25994|Lightjack Formation|49644|5|Briefly described|Table|||||||||
25994|Lightjack Formation|60386|5|Briefly described|p297|Guadalupian|Guadalupian|Roebuck/Canning Basin.Deltaic - nearshore - shelf and limestone nearshore-shelf.||Of Liveringa Group.||||
25994|Lightjack Formation|64643|5|Briefly described|p9|||Of Liveringa Group. Possibly disconformable on Noonkanbah Formation based on reworked palynological assemblages.||||||
25994|Lightjack Formation|64974|1|Redefined|p143, p148 Fig. 6|Kazanian|Ufimian|Of Liveringa Group. Geological Province: Canning Basin.||||||24-JUN-09
25994|Lightjack Formation|66949|4|Described|p4 Fig.2, p6-7, p22-24, p28, p31, p33-34|Guadalupian|Artinskian|See also p46-47 Appx.2, p56 Appx.3, p60 Appx.4; p70,75-76,78-79,81,88 Appx.5; p119-120 Appx.7. Redefined here; formerly Lightjack Member (Guppy et al., 1958). Type section detailed. Up to 300m thick; shallow marine to lagoonal and swampy deposits. Forms prominent strike ridges, breakaways, mesas and hills. Contains bivalves, brachiopods, trace fossils and plant fragments. Biostratigraphic zonation. Contains biodegraded tar sand, probably part of a migration pathway. Possible coal-bed methane and underground coal gas; coal resources are currently being reassessed. Available core detailed. TOC and Rock-Eval data.||Unit in Liveringa Group.||Conformably, locally disconformably, overlies Noonkanbah Formation. Is overlain conformably by Condren Sandstone or Hardman Formation.|Dominated by siltstone and calcareous to ferruginous sandstone; minor coal and fossiliferous units; pisolitic iron bodies, probably discontinuous.|04-NOV-15
25994|Lightjack Formation|67354|6|Mentioned|p72.|Permian|Permian|||||||
25994|Lightjack Formation|67888|6|Mentioned|p42|Triassic|Carboniferous|||||||
25994|Lightjack Formation|69182|6|Mentioned|Ch4 p9, Ch4 p15-p16|Guadalupian|Guadalupian|North Canning Basin. Ch4 p43, Ch4 p45, Ch4 p47, Ch4 p50-p58,Ch4 p74-p77, Ch4 p84-p88, Ch4 p90. ||||Overlies the Noonkanbah Formation. Overlain by the Liveringa Group.||
25994|Lightjack Formation|69312|6|Mentioned|p13 fig 13-14, p14 fig 15|||Canning Basin. ||||||
25994|Lightjack Formation|70774|5|Briefly described|p5 fig 3, p9|Capitanian|Roadian|Canning Basin.||Liveringa Group||||10-FEB-20
25994|Lightjack Formation|70837|5|Briefly described|p242,246|Guadalupian|Guadalupian|Of Canning Basin. CA-TIMS ages of 268.63 to 270.14 Ma (Mory etal., 2012), corresponding to D. ericianus zone.||||||
25994|Lightjack Formation|70878|5|Briefly described|p718, p722|Permian|Permian|Canning Basin. Roadian-Wordian age range from ammonoids and brachiopods; slightly younger palynomorphs towards top of the unit. Other, similar, geochronological ages given. Calibration of palynological ages (D. granulata).|269.20 +/- 0.03 Ma from tuffs near base.|Liveringa Group.|||Dominated by siltstone and calcareous to ferruginous sandstone, with minor coal and fossiliferous beds near the base; includes tuff layers.|10-FEB-20
25994|Lightjack Formation|71146|5|Briefly described|p9, p37|Guadalupian|Guadalupian|Canning Basin. Coal seams are thin and currently subeconomic.|269.1-268.9 +/- 0.1 Ma (IDTIMS)||||Coal seams.|
25994|Lightjack Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Liveringa Group.|||Fossiliferous, shallow marine micaceous and ferruginous mudstone, siltstone, shale, and thinly bedded fine to coarse quartzose sandstone and ferruginous shale, with concretions near the base.|
25994|Lightjack Formation|71623|4|Described|p343,344, 346, 349, p345 fig 2||Roadian|Canning Basin. Well dated marine strata. Part of Pearce Cycle. Includes Ufimian age ammonoid and Stage 5b to 5c microflora.||||Overlain unconformably by Condren Sandstone, Hardman Formation. Boundary relationships with [underlying] Noonkanbah Formation unclear.|Laminated siltstone, fine-grained sandstone with marine fossils & ironstone passing gradationally upward into plant-rich & sometimes coaly sandstone. Upper part shale & fossiliferous, fine-grained sandstones.|
25994|Lightjack Formation|71894|5|Briefly described|p4|Guadalupian|Guadalupian|Canning Basin.||||Overlies the Noonkanbah Formation. Overlain by the Liveringa Group. Unconformably overlain by the Blina Shale.|Mixed siliciclastics, sandstone and coal.|
25994|Lightjack Formation|72499|5|Briefly described|p7 Fig.6.|Guadalupian|Guadalupian|Located in the Fitzroy Trough.||||Overlies Noonkanbah Formation and underlies Liveringa Group.|Mixed siliciclastic and coal deposits.|
25994|Lightjack Formation|72505|5|Briefly described|p889-p890, p892-893, 897|Lopingian|Roadian|Canning Basin. Correlates with the Dulhuntyispora granulata zone to the Dulhuntyispora parvithola zone (Roadian - extendiing into Lopingian). Age previously assigned as Roadian-Wordian on the basis of ammonoid fossils and brachiopods. CA-IDTIMS dating of zircon from tuff near the base confirms broad ages indicated by macrofaunas.||Liveringa Group||Overlies the Noonkanbah Formation, Overlain by the Condren Sandstone and the Hardman Formation.|Pale-dark, carbonaceous siltstone with six thin tuffaceous kaolinite and smectite beds.|17-MAR-20
25994|Lightjack Formation|73117|5|Briefly described|p3, p111, p121|Guadalupian|Guadalupian|Canning Basin.||Liveringa Group||Underlain by Noonkanbah Formation.|Dominantly mixed siliciclastic and coal.|
77884|Lindsay Hill Formation|69595|4|Described|p8, p9 fig 5, p10 tbl 2, p12, p15.|Statherian|Orosirian|Barren Basin, Yilgarn Craton/ Eastern Biranup Zone.  Depositional environment unknown, potentially this unit was deposited in a distal fluvial to tidal sandflat or alternatively, a delta. Significant portions of this unit are made up of c. 1800 Ma detritus. Forms isolated ridges and outcrops. Maximum and minimum depositional ages. See also  p16 tbl 3, p18, p32, p32 fig 17, p34 fig 19, p35, p38, p57.|1990 +/- 15 Ma -1710-1650 Ma ||||Cross-bedded and ripple-marked quartz rich metasandstone and quartzite. Pebbly metaconglomerate and siltstone also occurs.|
77884|Lindsay Hill Formation|70089|6|Mentioned|p263|Paleoproterozoic|Paleoproterozoic|Tropicana Zone, NE Albany-Fraser Orogen.||||||
77884|Lindsay Hill Formation|70090|4|Described|p442,444-449,451-453,457-458|Statherian|Statherian|Geological province: Albany-Fraser Orogen, West Australian Craton. Of Barren Basin. Deposited in a broad, relatively shallow basin under moderate to high-energy, fluvial to shallow marine environments. Sedimentary protoliths deposited between 1710 Ma and 1650 Ma during Biranup Orogeny. Variably metamorphosed to upper greenschist to amphibolite facies. Maximum depositional age: c.1798 Ma. Minimum depositional age: unconstrained. 2750-2600 Ma detrital zircon age component is reflective of Yilgarn Craton, and more specifically, overalps in age and Hf isotope signatures of Kalgoorlie Terrane intrusive rocks. Archean detrital zircon age components include c. 2835, 2761, 2728, 2640, 2635 Ma. Also includes c. 1807 Ma zircons.|||||Cross-bedded quartz-rich sandstone, pebbly conglomerate, and siltstone.|
77884|Lindsay Hill Formation|70153|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|Barren Basin, Albany-Fraser Orogen.|1798 +/- 24 Ma (isotopic) - 1600 Ma (inferred).||||Quartzite and metasandstone, interbedded with metasiltstone; locally interbedded with metaconglomerate and pebbly metasandstone.|
77884|Lindsay Hill Formation|70182|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Barren Basin.||||||
77884|Lindsay Hill Formation|70256|5|Briefly described|p4-5|||Barren Basin. Geochronology by Spaggiari et al. (2014).|1752 +/- 19 Ma (maximum depositional age).|||Overlies Tropicana Gneiss locally.|Metasedimentary rocks.|
77884|Lindsay Hill Formation|70802|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Geological province: Albany-Fraser Orogen. Of Barren Basin. Events: Albany-Fraser Orogeny Stage II (1225-1140 Ma); Albany-Fraser Orogeny (1330-1140 Ma); Albany-Fraser Orogeny Stage I (1330-1260 Ma); Biranup Orogeny (1710-1620 Ma). Sample GSWA 182416 (metasandstone) yielded a weighted mean 207Pb/206Pb age of 1798+\-24 Ma, interpreted as maximum depositional age of the sandstone protolith. See 500k_interpgeop14_lut.csv, 250k_pre_mesozoic_interpgeop_lut.csv.|1798+\-24 Ma; 1600 Ma (inferred)||||Quartzite and metasandstone, interbedded with metasiltstone; locally interbedded with metaconglomerate and pebbly metasandstone|
77884|Lindsay Hill Formation|71270|4|Described|500k_interpgeop16_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: West Australian Craton. Events: Albany-Fraser Orogeny Stage II (1225 - 1140 Ma); Albany-Fraser Orogeny (1330 - 1140 Ma); Albany-Fraser Orogeny Stage I (1330 - 1260 Ma); Biranup Orogeny (1710 - 1620 Ma).|1752+\-19 Ma; 1600 Ma (inferred)||||Quartzite and metasandstone, interbedded with metasiltstone; locally interbedded with metaconglomerate and pebbly metasandstone|
77884|Lindsay Hill Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Barren Basin.|Max age 1752+/-19 Ma, min ~1600.||||Quartzite and metasandstone, interbedded with metasiltstone; locally interbedded with metaconglomerate and pebbly metasandstone.|
77884|Lindsay Hill Formation|73084|6|Mentioned|p12|||Albany-Fraser Orogen, Kepa Kurl Booya Province, Tropicana Zone.||||||
77859|Lindsays Basalt|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2726 - 2699 Ma (inferred).|Coolgardie Subgroup||Overlain by Hampton Hill Formation|Basalt; massive to pillowed; tholeiitic composition; minor komatiitic basalt and carbonaceous shale units; metamorphosed.|
77859|Lindsays Basalt|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2726-2699 Ma (inferred)|Unit of Coolgardie Subgroup.|||Basalt; massive to pillowed; tholeiitic composition; minor komatiitic basalt and carbonaceous shale units; metamorphosed|
77859|Lindsays Basalt|73391|5|Briefly described|p194, 244, Appendices.|||Standing and Castleden (2002). Regional stratigraphic correlation chart of other workers. Apparently occurs in all four Domains of the northeastern Kalgoorlie Terrane; unfortunately, its symbol and colour in the stratigraphic columns on p244 are identical with those for the Lower Basalt.||||Overlies Brilliant Ultramafic. Is overlain by Hampton Ultramafic, Siberia Komatiite, Kambalda Komatiite and Big Blow Chert.||
77859|Lindsays Basalt|73596|6|Mentioned|p1162|||Coolgardie Inlier, Kalgoorlie Terrane.||Coolgardie Subgroup.||Overlies Brilliant Formation. Is overlain by Hampton Hill Formation.||
29290|Linesman Formation|42710|5|Briefly described|map legend|Proterozoic||Variation on Linesman Beds.||Of Oscar Range Group||||17-OCT-12
29290|Linesman Formation|42811|4|Described|p29|Neoproterozoic|Mesoproterozoic|Of Oscar Range Group.  ~1300m thick.||||In fault contact with Christopher Formation to NE and Ellimberrie Formation to SW. Top of Ellendale Fm lithologically similar to base Linesman, so may be conformable.|Interbedded siltstone, feldspathic sandstone, quartz sandstone, and pebble and cobble conglomerate.|17-OCT-12
29290|Linesman Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Oscar Range Group.|||Grey-green and purple-grey siltstone and shale, buff feldspathic sandstone and minor boulder conglomerate|
27823|Lissadell Formation|22547|4|Described|p25||Mesoproterozoic|Of the Carr Boyd Group. Geological province: Carr Boyd Basin. Thickness: 1200 m. Overlies Golden Gate Siltstone, overlain by Glenhill Formation.||||||14-NOV-06
27823|Lissadell Formation|22754|5|Briefly described|p11 Tb. 3|Mesoproterozoic|Mesoproterozoic|Of the Carr Boyd Group||||||
27823|Lissadell Formation|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
27823|Lissadell Formation|32660|5|Briefly described|Table 6|||||||||
27823|Lissadell Formation|32664|6|Mentioned|Map legend|Adelaidean|Adelaidean|Mention in notes||||||
27823|Lissadell Formation|32728|6|Mentioned|p46|||||||||
27823|Lissadell Formation|36551|6|Mentioned|Table 12|||||||||
27823|Lissadell Formation|36885|4|Described|p179|||||||||
27823|Lissadell Formation|40813|6|Mentioned|p335|||||||||
27823|Lissadell Formation|41158|5|Briefly described|p39|||Mention P37||||||
27823|Lissadell Formation|41703|6|Mentioned|p232|||||||||
27823|Lissadell Formation|43853|5|Briefly described|Map Legend||Proterozoic|||||||
27823|Lissadell Formation|44155|5|Briefly described|p250 Tb.3-10|||Up to 1500m thick.||Carr Boyd Group||Unconformably overlies Golden Gate Siltstone. Is overlain unconformably by Glenhill Formation.|Blocky quartz sandstone; purple, green and grey micaceous quartz siltstone, shale and fine sandstone.|
27823|Lissadell Formation|44230|5|Briefly described|Map Legend||Proterozoic|||||||
27823|Lissadell Formation|44363|5|Briefly described|p.6,14,17,24|||(Adelaidean) Carr Boyd Group.||||||
27823|Lissadell Formation|44364|14|Not recorded|map legend|||||||||
27823|Lissadell Formation|45047|4|Described|p35|||||||||
27823|Lissadell Formation|45112|6|Mentioned|Table 16|||||||||
27823|Lissadell Formation|65417|5|Briefly described|pp156-159.|Mesoproterozoic|Mesoproterozoic|Halls Creek Orogen. Braided-delta progradation and retreat.||Unit in Carr Boyd Group.||Conformably overlies Golden Gate Siltstone. Is overlain conformably by Glenhill Formation.||
27823|Lissadell Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Carr Boyd Basin||Carr Boyd Group|Includes unnamed member||Fine- to coarse-grained, thin- to thick-bedded quartz sandstone; subordinate micaceous siltstone and mudstone.|31-JUL-15
27823|Lissadell Formation|69165|4|Described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic||||||Thin to thick bedded, fine to coarse grained quartz sandstone, micaceous siltstone and mudstone.|
27823|Lissadell Formation|69435|5|Briefly described|p20:3|||Carr Boyd Basin.||Carr Boyd Group.||Overlies Golden Gate Siltstone. Is overlain by Glenhill Formation.||12-JUL-16
27823|Lissadell Formation|69634|4|Described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Halls Creek Orogen. Of Carr Boyd Basin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1.|1200-1177 Ma (Inferred)|Unit of Carr Boyd Group.|||Fine- to coarse-grained quartz sandstone; subordinate micaceous siltstone and mudstone|
27823|Lissadell Formation|69673|6|Mentioned|p60 fig 48|||||Carr Boyd Group||Overlain by Glenhill Formation, overlies Golden Gate Siltstone||
27823|Lissadell Formation|70154|4|Described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic||1177-1200 Ma|Carr Boyd Group|||Fine to coarse grained quartz sandstone; subordinate micaceous siltstone and mudstone.|
27823|Lissadell Formation|70812|5|Briefly described|p23|Middle Proterozoic|Middle Proterozoic|||||||
27823|Lissadell Formation|71267|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Halls Creek Orogen. Of Carr Boyd Basin. Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1200-1177 Ma (inferred)|Unit of Carr Boyd Group.|||Fine- to coarse-grained, thin to thick-bedded quartz sandstone; subordinate micaceous siltstone and mudstone|
77861|Little Blow Member|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2726 - 2699 Ma (inferred).|Burbanks Formation|||Porphyritic tholeiitic basalt with rare pillows; feldspar phenocrysts; metamorphosed.|
77861|Little Blow Member|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2726-2699 Ma (inferred)|Unit of Burbanks Formation.|||Porphyritic tholeiitic basalt with rare pillows; feldspar phenocrysts; metamorphosed|
76057|Little Gap Suite|66195|5|Briefly described|p605, p598 Fig.1, p599 Fig.2,|Neoarchean||Yilgarn Craton.  500m thick sills of gabbroic rock, may represent subvolcanic component of Murrouli Basalt.|2792 +/- 5 Ma U-Pb zircon crystallisation date.|||Sills intrude Norie Group and Murrouli Basalt of the Polelle Group.||13-MAR-12
76057|Little Gap Suite|67129|5|Briefly described|p18 fig 19, p51-52|Archean|Archean|Murchison Domain, Youanmi Terrane. Volumetrically minor; not extensively explored.|2792 +/- 5 Ma|Annean Supersuite|||Mafic-ultramafic rocks.|07-SEP-17
76057|Little Gap Suite|68108|5|Briefly described|p651 Tb.4|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane.|2792 +/- 5 Ma; U-Pb (Ivanic et al. 2010).||||Differentiated igneous complexes.|
76057|Little Gap Suite|68110|5|Briefly described|p687|Neoarchean|Neoarchean|See also Little Gap Mafic-Ultramafic Suite (p674 Fig.2). Contemporaneous with Polelle Group.|c.2792 Ma.||||Volumetrically minor gabbroic sills.|
76057|Little Gap Suite|70020|6|Mentioned|p120|||Geological province: Youanmi Terrane, Yilgarn Craton.||||||
76057|Little Gap Suite|71311|6|Mentioned|p794|||Northern Youanmi Terrane, Yilgarn Craton.||||||
76057|Little Gap Suite|72491|6|Mentioned|p5 Fig.4|||Murchison Terrane, Yilgarn Craton.||||||
80719|Little Gold River Microgranite|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen, North Australian Craton.||Paperbark Supersuite.|||Microgranodiorite, micro-quartz diorite, and orthopyroxene-phyric andesite.|14-NOV-18
79018|Little Peters Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2682 - 2671 Ma (inferred).|Gindalbie Group|||Felsic volcanic and volcaniclastic rock; metamorphosed.|
79018|Little Peters Formation|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2682-2676 Ma (inferred)|Unit of Gindalbie Group.|||Felsic volcanic and volcaniclastic rock; metamorphosed|
73384|Little River Trondhjemite|63417|5|Briefly described|Map legend|Archean|Archean|Of the Cleland Supersuite. Geological Province: Pilbara Craton. Quartz-biotite trondhjemite and tonalite; leucocratic, massive, fine- to medium-grained, weakly metamorphosed.||||||07-NOV-08
73384|Little River Trondhjemite|65829|2|Defined|p7 Fig.3, p43.|Paleoarchean|Paleoarchean|New name. Named after Little River, a tributary of Yilgalong Creek. A faulted (western edge) semicircular intrusion on northeastern margin of exposed Yilgalong Granitic Complex. Type area along eastern side of Yilgalong Creek, 9.9 km southeast of Dingo Well.  Lack of deformation implies no significant post-3274 Ma deformation event in this eastern side of the Yilgalong Granitic Complex.|<c.3290 Ma.|Unit in Cleland Supersuite.||Intrudes Elsie Creek Tonalite. Is overlain unconformably by the Kylena Formation.|Massive, fine- to medium-grained leucocratic quartz trondhjemite.|
25997|Liveringa Group|7433|5|Briefly described|p25 Fig.2, pp37-38, p53.|Permian|Permian|Canning Basin.||||Includes basal Lightjack Formation.|Paralic facies; minor coal, carbonaceous shale.|
25997|Liveringa Group|13255|6|Mentioned|p369|Permian|Permian|Roebuck Basin. Late Permian.||||Overlies Noonkanbah Formation.||29-SEP-15
25997|Liveringa Group|13354|6|Mentioned|p376 Fig.7.|Late Permian|Early Permian|Onshore Canning Basin. Overlies Noonkanbah Formation and unconformably underlies Millyit Sandstone.||||||10-FEB-20
25997|Liveringa Group|22718|5|Briefly described|P5, Table1 P7|Late Permian|Early Permian|||||||
25997|Liveringa Group|22741|5|Briefly described|P28, Table3 P13||Late Permian|||||||
25997|Liveringa Group|22753|5|Briefly described|Fig.3 p585|Permian|Permian|||||||
25997|Liveringa Group|22764|5|Briefly described|Table 2, p9|Late Permian|Early Permian|Includes Condren sandstone, Lightjack Formation.||||||01-FEB-10
25997|Liveringa Group|22767|5|Briefly described|Table3 P14, P22||Late Permian|||||||
25997|Liveringa Group|22776|5|Briefly described|Table.3|Late Permian|Early Permian|||||||
25997|Liveringa Group|22814|5|Briefly described|fig2|Permian|Permian|||||||
25997|Liveringa Group|23765|5|Briefly described|Map Legend|Permian|Permian|||||||
25997|Liveringa Group|23766|4|Described|p14 Tb. 2|Permian|Permian|Interbedded sandstones, siltstone and shale. Max. thickness: 319m.  See also p20.||||||03-FEB-10
25997|Liveringa Group|24466|5|Briefly described|p372, p368 Fig. 3|Permian|Permian|||||||
25997|Liveringa Group|29806|6|Mentioned|Map legend|Permian|Permian|||||||
25997|Liveringa Group|29807|4|Described|Table 1|||||||||
25997|Liveringa Group|29813|6|Mentioned|p7|||||||||
25997|Liveringa Group|29817|4|Described|p7|||||||||
25997|Liveringa Group|29818|6|Mentioned|Map legend|Permian|Permian|||||||
25997|Liveringa Group|29819|6|Mentioned|Map legend|Permian|Permian|||||||
25997|Liveringa Group|33518|4|Described|Table 1|||||||||
25997|Liveringa Group|33519|6|Mentioned|Map legend|Permian|Permian|||||||
25997|Liveringa Group|33960|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
25997|Liveringa Group|33965|6|Mentioned|p14|||||||||
25997|Liveringa Group|33966|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
25997|Liveringa Group|35104|6|Mentioned|Fig.8|||||||||
25997|Liveringa Group|35120|6|Mentioned|Map legend|Late Permian|Early Permian|Early to Late||||||
25997|Liveringa Group|35124|6|Mentioned|Map legend|Late Permian|Early Permian|Early - Late Permian||||||
25997|Liveringa Group|35205|6|Mentioned|Map legend|Permian|Permian|||||||
25997|Liveringa Group|35873|6|Mentioned|Fig.38|||||||||
25997|Liveringa Group|36020|6|Mentioned|p392|||||||||
25997|Liveringa Group|36224|5|Briefly described|Map legend|Late Permian|Early Permian|Includes: Hardman and Lightjack Formations.||||||01-FEB-05
25997|Liveringa Group|36225|6|Mentioned|Map legend|Late Permian|Early Permian|Early to Late Permian||||||
25997|Liveringa Group|36257|6|Mentioned|Table 2.1|||||||||
25997|Liveringa Group|36634|6|Mentioned|Map legend|Late Permian|Early Permian|Early to Late Permian||||||
25997|Liveringa Group|38878|6|Mentioned|Map legend|Tatarian|Kazanian|Kungurian - Tatarian||||||
25997|Liveringa Group|38886|6|Mentioned|Map legend|Late Permian|Early Permian|Early to Late Permian||||||
25997|Liveringa Group|39169|6|Mentioned|p73|||||||||
25997|Liveringa Group|40045|6|Mentioned|Map legend|Late Permian|Early Permian|Early to Late Permian||||||
25997|Liveringa Group|40794|6|Mentioned|p91|||||||||
25997|Liveringa Group|40992|6|Mentioned|Fig.11|||||||||
25997|Liveringa Group|41158|6|Mentioned|p174|||||||||
25997|Liveringa Group|41215|6|Mentioned|p281|||||||||
25997|Liveringa Group|41449|5|Briefly described|p256|||||||||
25997|Liveringa Group|41688|4|Described|p10|||See also P22||||||
25997|Liveringa Group|41689|6|Mentioned|Table 1|||||||||
25997|Liveringa Group|41730|6|Mentioned|Fig.3|||||||||
25997|Liveringa Group|41809|6|Mentioned|p65|||||||||
25997|Liveringa Group|42347|6|Mentioned|Fig.2 P1020|||||||||
25997|Liveringa Group|42571|5|Briefly described|p20, Table1 p9|||||||||
25997|Liveringa Group|42613|6|Mentioned|P 18|||||||||
25997|Liveringa Group|42710|5|Briefly described|map legend|Permian||||||||
25997|Liveringa Group|42734|5|Briefly described|map legend|Permian||||||||
25997|Liveringa Group|42811|5|Briefly described|p45|||||||||
25997|Liveringa Group|42880|5|Briefly described|Fig.2,p1020|||||||||
25997|Liveringa Group|43050|5|Briefly described|p20|||||||||
25997|Liveringa Group|43173|5|Briefly described|12-54|Late Permian|Early Permian|||||||
25997|Liveringa Group|43281|5|Briefly described|Map legend||Permian|||||||
25997|Liveringa Group|43563|6|Mentioned|Fig.9,p15|Late Permian|Early Permian|||||||
25997|Liveringa Group|43656|6|Mentioned|Fig.2,p8|Dorashamian|Kungurian|||||||
25997|Liveringa Group|43666|6|Mentioned|p45,Table 2|Dorashamian|Kungurian|||||||
25997|Liveringa Group|43746|6|Mentioned|Fig.2,p11|Dorashamian|Kungurian|||||||
25997|Liveringa Group|43818|6|Mentioned|Fig.2.p39|Late Permian|Early Permian|||||||
25997|Liveringa Group|43932|5|Briefly described|p8,Tb.1 p6||Permian|||||||
25997|Liveringa Group|44143|4|Described|p435, p445|Permian|Permian|Includes Hardman and Lightjack Formations, Condren and Triwhite Sandstones. Sandstone, mudstone, conglomerate; minor coal or limestone.||||||23-NOV-17
25997|Liveringa Group|44231|5|Briefly described|Map Legend|Permian|Permian|Includes: Lightjack, Condren and Hardman Formations. Geological Province: Canning Basin.||||||26-MAY-05
25997|Liveringa Group|44356|5|Briefly described|p9,Tb.1 p6|||||||||
25997|Liveringa Group|44657|14|Not recorded|p.10|||(Fitzroy Basin).||||||
25997|Liveringa Group|45140|5|Briefly described|p67|Permian|Permian|Canning Basin.|||Lightjack Formation, Condren Sandstone.|||
25997|Liveringa Group|45149|6|Mentioned|p49|||||||||
25997|Liveringa Group|45153|2|Defined|App.4-72|Late Permian|Late Permian|Formerly Liveringa Sandstone, Liveringa beds & Liveringa Iron Sandstone.||||||
25997|Liveringa Group|45158|3|Fully described|p18|||See also p11.||||||05-NOV-15
25997|Liveringa Group|45168|6|Mentioned|p6|||||||||
25997|Liveringa Group|46849|6|Mentioned|p186|||||||||
25997|Liveringa Group|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
25997|Liveringa Group|48848|14|Not recorded|p.90|||||||||
25997|Liveringa Group|49644|5|Briefly described|Table|||||||||
25997|Liveringa Group|50544|5|Briefly described|p62|Permian|Permian|Overlies the Grant Group. Geological Province: Canning Basin.||||||03-FEB-10
25997|Liveringa Group|50555|5|Briefly described|Map legend|Permian|Permian|Sandstone and siltstone. Geological Province: Canning and Northern Carnarvon Basins (Westralian Superbasin).||||||03-FEB-10
25997|Liveringa Group|60386|5|Briefly described|p297|Lopingian|Guadalupian|Roebuck/Canning Basin.Includes volcanics dated at 253 +/-5 Ma. Deltaic - nearshore - shelf and limestone nearshore-shelf.|||Includes Lightjack Formation, Kirkby Radiolarite, Cherrabun Formation.|||
25997|Liveringa Group|61021|5|Briefly described|p36 Fig. 2|Tatarian|Kungurian|Geological Province: Canning Basin.||||||17-DEC-07
25997|Liveringa Group|61551|6|Mentioned|p351 Fig.2. |Lopingian|Kungurian|||||Overlies Noonkanbah Formation.||
25997|Liveringa Group|64187|5|Briefly described|p320 Fig. 2|Permian|Permian|Underlain by Noonkanbah Formation, overlain unconformably by Blina Shale.  Sandstone, siltstone, shale (marginal marine, marine). Geological Province: Canning Basin.||||||03-FEB-10
25997|Liveringa Group|64580|4|Described|map legend||Late Permian|Sandstone and siltstone, minor conglomerate and coal.||||||09-DEC-08
25997|Liveringa Group|64630|5|Briefly described|p31 Fig.2|Capitanian|Roadian|Province: Northern and Central Canning Basin. Overlies the Noonkanbah Formation. Palynology age: D. granulata to D. parvithola.||||||24-NOV-09
25997|Liveringa Group|64643|4|Described|p9, p3 Fig. 2, p5, fig.4, p20|Lopingian|Roadian|Middle to Upper Permian. Up to 435m thick in Fitzroy Trough. Possibly disconformable on Noonkanbah Formation, based on reworked pollen in Lightjack Formation.||||||17-NOV-08
25997|Liveringa Group|64974|5|Briefly described|p148 Fig. 6|Tatarian|Kungurian|Includes; Lightjack and Hardman Formations and Condren Sandstone. Geological Province: Canning Basin.||||||24-JUN-09
25997|Liveringa Group|65301|5|Briefly described|p3, p5 Fig. 4|Late Permian|Middle Permian|Geological province: Canning Basin.||||||
25997|Liveringa Group|65449|5|Briefly described|p5-6|Lopingian|Cisuralian|Deltaic deposits.||||Overlies Noonkanbah Formation. Is overlain unconformably by Millyit Sandstone.||
25997|Liveringa Group|66127|6|Mentioned|p251 Fig.334, Plates 4, 5, 7. |Permian|Permian|||||Overlies Noonkanbah Formation.|Well-bedded, shallow-marine to fluvial sandstone and siltstone; ferruginous in part.|
25997|Liveringa Group|66949|4|Described|p6-7, p23-24, p26, p28, p31, p34|Permian|Permian|See also p47,51-52 Appx.2, p55 Appx.3, p60-65 Appx.4; p66,68,76,78-80,82-83,85-88,90-92,94 Appx.5; p119-120 Appx.7; Plates 2-6,10,12. Originally referred to as Upper Ferruginous or Liveringa Series by Wade (1937); later as Liveringa Sandstone (Guppy et al., 1950). Reeves (1951) wrote of the Liveringa beds [including the Liveringa sandstone and Belina shale]. Guppy et al. (1951) redefined these as the Liveringa Group, including the Liveringa Iron Sandstone, Belina Shale and Erskine Sandstone (of Kraus, 1942, and Findlay, 1942). Guppy et al. (1958) subsequently reduced it to the Liveringa Formation. In 1975 it was reinstated to Group status by Yeates et al. Type section detailed. Up to ?1000m thick; shallow marine to fluvial deposits. Biostratigraphic zonation. Unlikely hydrocarbon source or seal. Available core and Formation picks detailed. TOC and Rock-Eval data.|||Includes Lightjack and Hardman Formations and Condren Sandstone.|Overlies Noonkanbah Formation.|Sandstone and mudstone; minor coal and limestone. Basalt intersected in Corbett 1 well.|
25997|Liveringa Group|67202|5|Briefly described|p67|Permian|Permian||||Poole, Triwhite Sandstones; Noonkanbah Formation.||Sandstone and siltstone.|15-FEB-18
25997|Liveringa Group|68007|5|Briefly described|p2, p4, p9, p12, p14-15, Plate 2|Permian|Permian|Canning Basin. 114m thick (undifferentiated) in Patience 1 and 2 wells. Fluvial setting with channel sands and swampy alluvial plains. Reservoir potential. Composite well log. Middle to Late Permian. Wordian palynomorphs D. ericianus Zone at 280m Patience 1 (Backhouse, 1997). Sharp (unconformable) top boundary with overlying Mesozoic rocks. Shown as Liveringa Formation in Plate 1.||||Overlies Noonkanbah Formation transitionally.|An interbedded succession of sandstone, siltstone and minor coal. Sandstone is yellowish-grey, very fine- to coarse-grained, moderately sorted, commonly carbonaceous, pyritic and micaceous; siltstone is micaceous and carbonaceous, grading to lignite.|19-FEB-20
25997|Liveringa Group|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Lopingian|Guadalupian|Canning Basin. See also 500k_geologyp08_lut.csv.|||||Sandstone and siltstone, minor conglomerate, and coal|
25997|Liveringa Group|68902|5|Briefly described|p8, p9 fig 5, p24|Permian|Permian|Not known from boreholes within Waukarlycarly Embayment, but has been intersected in northern Wallal Embayment.||||Overlies Noonkanbah Formation; overlain unconformably by Millyit Sandstone.||
25997|Liveringa Group|69029|6|Mentioned|p319|Wuchiapingian|Kungurian|Of Canning Basin.||||Overlain by Blina Shale. Underlain by Noonkanbah Formation.||
25997|Liveringa Group|69099|5|Briefly described|500k_geologyp08_lut.csv||Late Permian||||||Sandstone and siltstone, minor conglomerate and coal.|31-JUL-15
25997|Liveringa Group|69165|4|Described|500k_geologyp08_lut.csv|Permian|Permian||||||Undivided; sandstone and siltstone, minor conglomerate and coal.|
25997|Liveringa Group|69182|5|Briefly described|Ch4 p3, Ch4 p9, Ch4 p15-p16|Lopingian|Guadalupian|Canning Basin. See also Ch4 p30-p35, Ch4 p38, Ch4 p43-p45, Ch4 p47, Ch4 p50-p58, Ch4 p63-p64, Ch4 p74-p77, Ch4 p83-p84, Ch4 p88, Ch4 p90. ||||Overlies the Lightjack Formation. Unconformably overlain by the Millyit Sandstone.|Sandstones and claystones with minor fossiliferous limestones.|
25997|Liveringa Group|69297|6|Mentioned|p337, p351, p352, p354|Wordian|Roadian|Roebuck Basin. ||||Overlies the Noonkanbah Formation. Unconformably overlain by the Bedout Volcanics.||
25997|Liveringa Group|69312|5|Briefly described|p3, p23 fig 27|Changhsingian|Roadian|Canning Basin. See also p24 fig 28-29, p26 fig 33, p27, p27 fig 34, p28 fig 35. ||||Overlies the Noonkanbah Formation. Overlain by the Blina Shale.|Carbonate shales, marl.|
25997|Liveringa Group|69587|4|Described|GEOL_LUT_CSV files|Lopingian|Guadalupian|Of Canning Basin. Events: Alice Springs Orogeny; Point Moody Extension; Prices Creek Movement; Red Bluffs Extension; Van Emmerick Extension. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|272.3-252.2 Ma (biostrat)||||Sandstone and siltstone, minor conglomerate, and coal|
25997|Liveringa Group|69634|5|Briefly described|500k_geologyp08_lut.csv||Late Permian||||||Undivided; sandstone and siltstone, minor conglomerate and coal|
25997|Liveringa Group|69693|5|Briefly described|p3-4|Permian|Permian|Canning Basin. Guadalupian to Lopingian.||||Overlies Noonkanbah Formation.|Post-glacial fluvial to marine siliciclastic sediments.|
25997|Liveringa Group|70065|5|Briefly described|Rowley: Fig.2. Regional: Fig.4; p3|Guadalupian|Guadalupian|Roebuck Basin.||||Overlies Noonkanbah Formation. Is overlain by Bedout Volcanics.||
25997|Liveringa Group|70129|5|Briefly described|Map legend|Permian|Permian|Canning Basin.|||||Sandstone and siltstone, minor conglomerate, and coal (section only).|
25997|Liveringa Group|70154|5|Briefly described|500k_interpgeop14_lut.csv|Lopingian|Guadalupian||252-272 Ma||||Sandstone and siltstone, minor conglomerate, and coal|
25997|Liveringa Group|70762|5|Briefly described|Map legend.|Permian|Permian|Canning Basin.|||||Sandstone and siltstone; minor conglomerate and coal.|
25997|Liveringa Group|70774|5|Briefly described|p4-p5, p8-p9, p34|Lopingian|Cisuralian|Fitzroy Trough, Lennard Shelf and Willara and Kidson Sub-basins, Canning Basin.|||Includes the Lightjack Formation, Hardman Formation, Condren Sandstone..|Conformably overlies the Noonkanbah Formation. Overlain by the Millyit Sandstone.||10-FEB-20
25997|Liveringa Group|70826|6|Mentioned|p6 tbl 3|Permian|Permian|Canning Basin.||||||
25997|Liveringa Group|70878|5|Briefly described|p722 Fig.17|Permian|Permian|Fitzroy Trough, NW Canning Basin.|||Lightjack Formation.|||
25997|Liveringa Group|71146|5|Briefly described|p6, p12 fig 8, p37|Guadalupian|Guadalupian|Canning Basin.|||||Carbonate and mudstone.|
25997|Liveringa Group|71267|4|Described|GEOL_LUT_CSV files|Lopingian|Guadalupian|Of Canning Basin. Events: Point Moody Extension (300-242 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|272.3-242.17  Ma (biostrat)||Includes Condren Sandstone, Lightjack Formation.||Interbedded sandstones, siltstone and shale.|
25997|Liveringa Group|71870|6|Mentioned|p3|Changhsingian|Kungurian|Canning Basin.||||Overlies the Noonkanbah Formation.||
25997|Liveringa Group|71894|5|Briefly described|p4|Guadalupian|Guadalupian|Canning Basin.||||Overlies the Lightjack Formation. Disconformably overlain by the Millyit Sandstone.|Carbonate, shale and sandstone.|
25997|Liveringa Group|72034|5|Briefly described|500k_interpgeop16_lut|Lopingian|Guadalupian|Canning Basin.  Age from biostratigraphy.|||||Sandstone and siltstone, minor conglomerate, and coal.|
25997|Liveringa Group|72496|6|Mentioned|p220|Wuchiapingian|Kungurian|Canning Basin. Deposited in a shallow marine to fluvial environment.||||Overlies the Noonkanbah Formation.||
25997|Liveringa Group|72497|5|Briefly described|p3 Fig.2.|Wuchiapingian|Kungurian|Shown as occuring in the Anketell, Tabletop, Ryan Shelves, Willara and Kidson Sub-basins, the Jurgurra and Barbwire Terraces and Broome Platform. Also shown as occuring in the Fitzroy Trough, Betty and Balgo Terraces and part of the Lennard Shelf and Margaret Terrace. Top of unit diachronous. Younger to north. Age shown as Kungurian to Dzhulfian = Kungurian-Wuchiapingian.||||Conformably overlies Noonkanbah Formation.||
25997|Liveringa Group|72499|4|Described|p7, p8, p43, p53, p95-96.|Lopingian|Guadalupian|Located in the Fitzroy Trough and Lennard Shelf. Shown at the top of the Sisters 1 well log p96, also in Frome Rocks 2, Scarpia 1, Sundown 3, p53. See also Liveringa Formation well logs Sundown 1 and Sundown 3/3H (Lennard Shelf) and Scarpia 1 (Fitzroy Trough) p54.||||Overlies Lightjack Formation and underlies Millyit Sandstone.|Includes carbonate shales, ?and sandstones.|
25997|Liveringa Group|72505|5|Briefly described|p890|Wuchiapingian|Roadian|Canning Basin. Correlates to the Dulhuntyispora granulata zone to the Dulhuntyispora parvithola zones.|||Includes the Lightjack Formation, Condren Sandstone and the Hardman Formation.|Overlies the Noonkanbah Formation. Unconformably overlain by the Blina Shale.||17-MAR-20
25997|Liveringa Group|73117|5|Briefly described|p3, p34, p116, p125, p127, p135-140|Lopingian|Guadalupian|Canning Basin.|||Lightjack Formation|Underlain by Noonkanbah Formation. Disconformably overlain by Millyit Sandstone.|Includes sandstone, carbonate-shale, marl, mixed siliciclastic and coal.|
25997|Liveringa Group|73445|5|Briefly described|p3, 6, 8, 12-14, 18, 20, 23-27, 29-30|Paleozoic|Paleozoic|See also p34, 36-38, 41-47, 50-53, 56, 65-118. Canning Basin. 620m thick. Whole-rock and regolith chemistries tabulated in detail. Multi-element spider diagram. Appears also as Liveringa Formation on p41. Commonly forms surface ferruginous lag (chemistry discussed).||||Overlies Noonkanbah Formation. Is overlain disconformably by Millyit Sandstone.|Sandstone and siltstone, minor conglomerate and coal.|
38689|Lizard Hills Formation|23789|5|Briefly described|p10 Tb. 3|||Geological Province: Pilbara Craton.||||||
38689|Lizard Hills Formation|24391|4|Described|p8-2|Archean|Archean|Geological Province: Pilbara Block. Overlies Lagoon Pillow Basalt unconformably. Clastic sediments. Overlain by Fortescue Group.||||||07-NOV-08
38689|Lizard Hills Formation|68574|6|Mentioned|p3-5|||Kiyokawa and Taira (1998).|||Forty-four Hill, Sixty-six Hill, Members.|||
22208|Loadstone Monzogranite|22496|5|Briefly described|p8|Orosirian|Paleoproterozoic|||||||07-NOV-08
22208|Loadstone Monzogranite|22754|5|Briefly described|p7|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  Age: 1827 Ma.||||||07-NOV-08
22208|Loadstone Monzogranite|23383|4|Described|p14, p5 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Sally Downs supersuite (Lamboo Complex).  Almost entirely medium- to coarse-grained, weakly porpyritic biotite monzogranite and syenogranite.  Intrudes the Lamboo Ultramafics.  Age: 1827 +/- 2 Ma (SHRIMP U-Pb). Geol.Proc: Halls Creek Orogen.||||||07-NOV-08
22208|Loadstone Monzogranite|23599|4|Described|p12|Paleoproterozoic|Paleoproterozoic|Age: c.1827 Ma. See also page 5 Table 1. Of Sally Downs supersuite.||||||07-NOV-08
22208|Loadstone Monzogranite|23601|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|In the Lamboo Complex.  Weakly porphyritic biotite monzogranite and syenogranite; minor microgranodiorite.||||||07-NOV-08
22208|Loadstone Monzogranite|23621|2|Defined|p53 Appendix|Orosirian|Orosirian|See also page 20, 10 table 1. Age: 1827+/-2 Ma (U-Pb zircon). Of Sally Downs supersuite. Geological Province: Bow River Batholith.||||||
22208|Loadstone Monzogranite|23622|5|Briefly described|Map Legend|Orosirian|Orosirian|Age: c 1827 Ma. Geological Province: Bow River Batholith.||||||
22208|Loadstone Monzogranite|24173|4|Described|p20, p12 Tb.2|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs Supersuite. Geological Province: Halls Creek Orogen. Previously mapped as Bow River Granite (Gemuts & Smith, 1968). Intrudes the Koongie Park Formation. Age: c.1827 +/- 2Ma||||||07-NOV-08
22208|Loadstone Monzogranite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs Supersuite. Age: 1825Ma. Geological province: Kimberley Province.||||||07-FEB-11
22208|Loadstone Monzogranite|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.Weakly porphyritic biotite monzogranite and syenogranite; minor microgranodiorite. Age: 1835-1805Ma. Part of the Bow River batholith.||||||07-NOV-08
22208|Loadstone Monzogranite|44693|5|Briefly described|Map Legend||Proterozoic|||||||
22208|Loadstone Monzogranite|44694|5|Briefly described|Map Legend||Proterozoic|||||||
22208|Loadstone Monzogranite|50437|5|Briefly described|p1.6, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Kevins Dam Suite (Sally Downs Supersuite). Age: 1827 +/- 2Ma (Shrimp).||||||07-NOV-08
22208|Loadstone Monzogranite|66845|4|Described|p537, p539 Tb.1, p541-3, Figs. 3, 6, 9|||Five measured zircon cores have a range in 207Pb/206Pb ages: 2220, 1914, 1874, 1870 and 1886 Ma reflecting inheritance from source or crustal contamination. Abundant, morphologically complex zircons with numerous clear cores, and zoned and unzoned rims.|20 analyses, magmatic age 1827+/-4 Ma SHRIMP U-Pb|Kevins Dam suite|||biotite monzogranite|
22208|Loadstone Monzogranite|66846|5|Briefly described|p558 Table 4|Orosirian|Orosirian|Age probably from U-Pb SHRIMP dating of zircon (see p547). |~1827 Ma|Of Kevins Dam suite.||||
22208|Loadstone Monzogranite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Data from OZCHRON1. Comment: 'This magmatic crystallisation age is derived from 20 of the 27 data points|crystallisation age 1827+/-4 Ma U/Pb SHRIMP|Kevins Dam Suite|||Weakly porphyritic biotite monzogranite and syenogranite; minor microgranodiorite.|31-JUL-15
22208|Loadstone Monzogranite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv. |1827 Ma|Kevins Dam Suite|||Weakly porphyritic biotite monzogranite and syenogranite; minor microgranodiorite.|
22208|Loadstone Monzogranite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2.|1827-1827 Ma (Isotopic)|Unit of Kevins Dam Suite.|||Weakly porphyritic biotite monzogranite and syenogranite; minor microgranodiorite|
22208|Loadstone Monzogranite|70154|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv.|1808-1827 Ma|Kevins Dam Suite|||Weakly porphyritic biotite monzogranite and syenogranite; minor microgranodiorite|
22208|Loadstone Monzogranite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1827+\-4 Ma (isotopic)|Unit of Kevins Dam Suite.|||Weakly porphyritic biotite monzogranite and syenogranite; minor microgranodiorite|
22208|Loadstone Monzogranite|72437|5|Briefly described|p104|||Whole rock analyses are provided.||Kevins Dam Suite|||Biotite monzogranite.|
23735|Logue Brook Granite|23785|5|Briefly described|p8|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
23735|Logue Brook Granite|23788|5|Briefly described|p16|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
23735|Logue Brook Granite|24542|5|Briefly described|p12|Archean|Archean|Age: 2575 Ma (Rb-Sr). Porphyritic.||||||07-NOV-08
23735|Logue Brook Granite|38769|4|Described|p72|||||||||
23735|Logue Brook Granite|39897|6|Mentioned|p78|||||||||
23735|Logue Brook Granite|40358|6|Mentioned|p15|||||||||
23735|Logue Brook Granite|40359|6|Mentioned|p8|||||||||
23735|Logue Brook Granite|40667|6|Mentioned|p193|||||||||
23735|Logue Brook Granite|43052|5|Briefly described|Fig.3.8|||||||||
23735|Logue Brook Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
23735|Logue Brook Granite|73057|6|Mentioned|p3, p9|Neoarchean|Neoarchean|Yilgarn Craton. Ca 2612 age may represent recrystallisation age.|ca. 2612-2611 Ma|||||
74630|Lombadina Conglomerate Member|64449|2|Defined|p75, p76, p79 Tb. 5, p87, p89|Holocene|Holocene|Of Cable Beach Sand. Reworked beachrock forming rounded slabs and breccia, pebble to boulder size. See p79 Tb. 5 for more information.||||||07-FEB-11
26699|Lone Hand Monzogranite|42696|6|Mentioned|Plate 1B|Archean||Reserved as Lone Hand Granite.||||||07-NOV-08
26699|Lone Hand Monzogranite|43232|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
26699|Lone Hand Monzogranite|60076|6|Mentioned|p45 App. 1|||[Agmon]   Leucogranite; massive.||||||
26699|Lone Hand Monzogranite|65204|6|Mentioned|p19 Tbl.4,|Neoarchean||?medium grains; equigranular.||||||
26699|Lone Hand Monzogranite|65264|5|Briefly described|p48 Appdx. 1|Archean|Archean|Leucocratic monzogranite; massive; contacts discordant with greenstones and foliation in early granite.||||||07-FEB-11
26699|Lone Hand Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Leucocratic monzogranite; massive; contacts discordant with greenstones and foliation in early granite.|06-AUG-15
26699|Lone Hand Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Leucocratic monzogranite; massive; contacts discordant with greenstones and foliation in early granite.|
26699|Lone Hand Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
26699|Lone Hand Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|3010-2600 Ma (inferred)||||Leucocratic monzogranite; massive; contacts discordant with greenstones and foliation in early granite|
26699|Lone Hand Monzogranite|73391|6|Mentioned|p304|||Ora Banda area.||||||
83649|Long Point basaltic dyke|73480|5|Briefly described|p214||Tonian|Vertical and N-NW striking dyke. See also Long Point dyke p208, 216-218. Hosted in sheared ortho- and paragneiss.|910+/-11 Ma U-Pb zircon maximum crystallisation||||Porphyritic basalt dyke.|
74806|Lordy Basalt Member|64891|5|Briefly described|p39, p48-9 Tb. 1|Archean|Archean|Previously Lordy Basalt of Watkins and Hickman (1990). Of the Meekatharra Formation. Situated at the base of the Polelle Group. Overlain by Stockyard Basalt Member. Age: c.2790Ma. Geol. prov: Murchison Domain. Komatiitic basalt in the Polelle Syncline.||||||07-FEB-11
74806|Lordy Basalt Member|67129|5|Briefly described|p18 Fig.19|Archean|Archean|Murchison Domain, Youanmi Terrane.||Meekatharra Formation.||||
74806|Lordy Basalt Member|68110|5|Briefly described|p674 Fig. 2|Neoarchean|Neoarchean|Murchison Domain.|c. 2792 Ma|Of the Meekatharra Formation.||Is overlain conformably by Stockyard Basalt Member.|Komatiitic basalt.|09-OCT-14
74806|Lordy Basalt Member|69583|5|Briefly described|p49|Neoarchean|Neoarchean|Murchison Domain.||Meekatharra Formation.||||
74806|Lordy Basalt Member|69584|5|Briefly described|p5 Fig.2|Neoarchean|Neoarchean|||Meekatharra Formation||Overlain by the Stockyard Basalt. Overlies the Coodardy and Mougooderra Formations.|Komatiite and komatiitic basalt.|
74806|Lordy Basalt Member|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Meekatharra Formation.||||
74806|Lordy Basalt Member|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.|2800-2760 Ma|Unit of Meekatharra Formation.|||Mafic volcanic rock, dominantly komatiitic basalt; massive to weakly foliated; locally pillowed and/or vesicular; metamorphosed|
74806|Lordy Basalt Member|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.||Meekatharra Formation.|||Mafic volcanic rock, dominantly komatiitic basalt; massive to weakly foliated; locally pillowed or vesicular; metamorphosed.|
74806|Lordy Basalt Member|72389|5|Briefly described|Map Legend|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Gabanintha 1:100k map sheet 2644.||Meekatharra Formation|||Mafic volcanic rock, dominantly komatiitic basalt; massive to weakly foliated; locally pillowed and/or vesicular; metamorphosed.|28-AUG-20
69178|Loreto Aplite|60623|5|Briefly described|p30|Archean|Archean|Age: 2687+/-4 Ma.||||||07-NOV-08
24365|Louden Volcanics|22449|6|Mentioned|P28, Fig27, P27||Archean|Age of unit is 3000 Ma||||||07-NOV-08
24365|Louden Volcanics|22471|5|Briefly described|27|Archean|Archean|Geol province Pilbara||||||07-NOV-08
24365|Louden Volcanics|22715|5|Briefly described|table7, fig7|Archean|Archean|Age: 2920Ma||||||07-NOV-08
24365|Louden Volcanics|23033|5|Briefly described|157|||||||||
24365|Louden Volcanics|23046|5|Briefly described|175|||Overlying unit Kialrah Rhyolite, underlying unit Whim Creek Group||||||
24365|Louden Volcanics|23244|5|Briefly described|Fig.2,5 p22|||of Whim Creek Belt. Overlying unit Mount Negri Volcanics.||||||
24365|Louden Volcanics|23348|5|Briefly described|220|||||||||
24365|Louden Volcanics|23484|4|Described|p10 table 3|Archean|Archean|Of Whim Creek Group.  Maximum thickness:  ~300m.  Geological Province: Mallina Basin.||||||07-NOV-08
24365|Louden Volcanics|23598|4|Described|p10|Archean|Archean|Defined Hickman 1990. Overlain by Kialrah Rhyolite. Underlain by Whim Creek Group. Max. thickness: 1300 m.||||||07-NOV-08
24365|Louden Volcanics|23743|6|Mentioned|p3|||Geological Province: Pilbara Craton.||||||
24365|Louden Volcanics|23784|5|Briefly described|p20|Archean|Archean|Of Bookingarra Group.||||||07-NOV-08
24365|Louden Volcanics|23789|5|Briefly described|p18 Tb. 4|Archean|Archean|Of Bookingarra Group.  Max. thickness: 2000m.  Geological Province: Pilbara Craton.||||||07-NOV-08
24365|Louden Volcanics|23793|4|Described|p27|Archean|Archean|Of Bookingarra Group||||||07-NOV-08
24365|Louden Volcanics|23794|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup. Geological Province Pilbara Craton.||||||07-NOV-08
24365|Louden Volcanics|23813|5|Briefly described|p90 Tb. 1|Archean|Archean|Of the Bookingarra Group.  Age: 2.965-2.95Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.||||||07-NOV-08
24365|Louden Volcanics|23936|4|Described|p9, Tb.1, Fig.4|Archean|Archean|Geological Province: Pilbara Craton. Age: c.3.0-2.925 Ga. Grouped with Mount Negri Volcanics and Kialrah Rhyolite in Table 1 as c.3.0-2.925 Ga.||||||21-FEB-17
24365|Louden Volcanics|24023|4|Described|p19|Archean|Archean|Of Bookingarra Group. Geological Province: Pilbara Craton. Maximum Thickness: 1000m.||||||07-NOV-08
24365|Louden Volcanics|24024|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
24365|Louden Volcanics|24140|6|Mentioned|p217 Fig. 2|||Together with Negri Volcanics, superseded by Mount Negri Volcanics in this study.  Interpreted as a separate basalt from Negri Volcanics by Fitton et al (1975) and Barley (1987) and inc. in Whim Creek Group then.||||||14-SEP-05
24365|Louden Volcanics|24169|5|Briefly described|p666 Fig. 5|||||||||
24365|Louden Volcanics|24184|4|Described|p715|Archean|Archean|Of the Bookingarra Group. Overlain by Kialrah Rhyolite. Underlain by Rushall Slate. Geological Province: Mallina Basin. Formerly included in Whim Creek Group (Hickman 1983), now assigned to the Bookingarra Group (Smithies et al, 2000)||||||07-NOV-08
24365|Louden Volcanics|24191|4|Described|p828 Fig. 1|Archean|Archean|Of Bookingarra Group.  Subaqueous basalt sheet lava up to 2m thick; pillow lava, hyaloclastite with intercalated massive quartz and laminated shale.  Overlies Mount Negri Volcanics; overlain by Kialrah Rhyolite.  Geological Province: Pilbara Craton.||||||07-NOV-08
24365|Louden Volcanics|24353|4|Described|p5|Archean|Archean|Overlying Unit: Kialrah Rhyolite. Underlying Unit: Whim Creek Group. Geological Province: Pilbara Craton||||||07-NOV-08
24365|Louden Volcanics|24410|6|Mentioned|p200 Fig. 138|Archean|Archean|||||||07-NOV-08
24365|Louden Volcanics|24550|5|Briefly described|p36 Tb. 3.2|Archean|Archean|Of the Bookingarra Group. Mainly mafic volcanics. Geological Province: Pilbara Craton.||||||07-FEB-11
24365|Louden Volcanics|38498|5|Briefly described|Table 1|||||||||
24365|Louden Volcanics|38544|6|Mentioned|Fig.1|||||||||
24365|Louden Volcanics|39672|6|Mentioned|Fig.2|||||||||
24365|Louden Volcanics|39697|2|Defined|p111|Archean|Archean|||||||07-NOV-08
24365|Louden Volcanics|39837|6|Mentioned|Table 1|||||||||
24365|Louden Volcanics|40596|6|Mentioned|Fig.1|||||||||
24365|Louden Volcanics|41250|5|Briefly described|Table 1|||||||||
24365|Louden Volcanics|41263|6|Mentioned|p57|||||||||
24365|Louden Volcanics|42329|4|Described|p5|||||||||
24365|Louden Volcanics|43052|5|Briefly described|Fig.3.8|||||||||
24365|Louden Volcanics|43595|6|Mentioned|p213|||||||||
24365|Louden Volcanics|43698|6|Mentioned|p3|||||||||
24365|Louden Volcanics|43821|5|Briefly described|map legend|Archean|Archean|Of Pilbara Supergroup||||||07-NOV-08
24365|Louden Volcanics|44150|5|Briefly described|p129 Tb.2-15, p132 Fig.2-131, p137|||See also p152 Tb.2-22. Faulted contact with other units.||Pilbara Supergroup||Overlies Whim Creek Group. Is overlain unconformably by Mount Negri Volcanics or Mount Roe Basalt.|Succession of intermediate, basaltic and ultramafic volcanic and intrusive rocks; pillow basalts are abundant and generally vesicular.|
24365|Louden Volcanics|44837|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
24365|Louden Volcanics|44863|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
24365|Louden Volcanics|46319|5|Briefly described|p4|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
24365|Louden Volcanics|60362|5|Briefly described|p1516-1531, p1533|Archean|Archean|NW Mallina Basin. Geochemistry detailed and tabulated.||Bookingarra Group.|||Subaqueous flows of high-Si basalts. Has undergone significant recrystallisation. Local well-developed pyroxene spinifex textures.|
24365|Louden Volcanics|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Age: >2.9Ga. Collectively referred to as Louden/Negri Volcanics in this study.  Geological Province: Pilbara Craton.||||||07-NOV-08
24365|Louden Volcanics|61267|5|Briefly described|p72 Fig.1|||Geological Province: Pilbara Craton.||||||
24365|Louden Volcanics|63372|4|Described|Map Legend|Archean|Archean|Of the Bookingarra Group. Geological Province: Whim Creek and Mallina Basin. Age: 2975-2945Ma. Undivided basalt, komatiitic basalt, and pyroxene spinifex-textured basalt; interbedded clastic units and chert; metamorphosed.||||||07-NOV-08
24365|Louden Volcanics|63441|3|Fully described|p6 Tb. 1, p27|Archean|Archean|Formerly of Bookingarra Group; now redefined as Louden Volcanic Member of Bookingarra Formation (Croydon Group, De Grey Supergroup). Overlies Cistern Fm. Thickness: up to 1300m. Geol.prov: Pilbara Craton. Predominantly metamorphosed komatiitic basalt.||||||07-FEB-11
24365|Louden Volcanics|63538|5|Briefly described|p7|Archean|Archean|Underlain by Cistern Formation. Geological Province: Pilbara Craton.||||||17-APR-13
24365|Louden Volcanics|65415|4|Described|p119 Fig.1, p120 Fig.2, p121.|Archean|Archean|Low TiO2 compared with Mount Negri Volcanics. The Opaline Well Complex may represent sub-volcanic equivalents to this unit. Mis-spelt as Lounden Volcanics on p121.||Unit in Pilbara Supergroup.||Conformably overlies Whim Creek Group. Is overlain unconformably by Mount Negri Volcanics.|Olivine and pyroxene spinifex-textured suite of basalts.|
24365|Louden Volcanics|69299|5|Briefly described|p6 Tb.1|Archean|Archean|Thickness on COOYA POOYA: 0-1000 m.||Of Bookingarra Group.||Is overlain by or intruded by Kialrah Rhyolite.|High-Mg basalt with pyroxene spinifex texture, and undivided massive and pillow basalt.|
24365|Louden Volcanics|69300|5|Briefly described|map legend|Archean|Archean|Mallina Basin, Whim Creek greenstone belt.||Bookingarra Group|||metamorphosed basalt and high-Mg basalt; metamorphosed interbedded clastic units and chert|
24365|Louden Volcanics|70775|4|Described|p12, p15, p24 tbl 3, p95-p96, p100|Mesoarchean|Mesoarchean|Mallina Basin. Name is derived from Louden Creek. The type area is 6km south-southwest of Mons Cupri (Hickman, 1983). An age of 2950 Ma is also given by Smithies et al., 2004a and a minimum age is given by the overlying Kialrah Rhyolite. Renamed as the Louden Volcanic Member (Van Kranendonk et al., 2006) before being redefined as the Louden Volcanics (Appendix, p96). This formation is exposed along the entire 110km length of the Whim Creek greenstone belt from Mount Ada, 15km south of Roebourne to Peawah River, 20km northeast of Whim Creek mine. The total outcrop area is approximately 400km ^2 and the depositional extent exceeded 2000km ^2.This formation has a maximum thickness of approximately 2000m. See also p29 tbl 5, p41, p45-p46, p51, p54-p56, p60-p61, p63, p65, p76.|c. 2950 Ma (Arndt et al, 2001)|Bookingarra Group||Unconformably overlies the Rushall Slate and Cistern Formation. Overlain by the Mount Negri Volcanics and the Kialrah Rhyolite. Unconformably overlain by the Mount Roe Basalt.|Basalt and komatiite with locally thick siliciclastic sedimentary intercalations; metamorphosed. Hyaloclastite and pillowed basalt are present and are interlayered with and conformably overlain by chert and clastic rocks, including conglomerate.|
24365|Louden Volcanics|72251|5|Briefly described|p54|||Geological province: West Pilbara Superterrane, Pilbara Craton.||||Contemporaneous with Sisters Supersuite.||
30670|Louisa Monzogranite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1860Ma. Geological province: Kimberley Province (West).||||||07-FEB-11
30670|Louisa Monzogranite|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|Approx 1865 - 1850 Ma.||||||
30670|Louisa Monzogranite|44231|5|Briefly described|Map Legend||Proterozoic|Of the Paperbark supersuite. Coarsely porphyritic syenogranite and monzogranite. Age: 1865-1850Ma.  In the Hooper Complex and Lamboo Complex western zone.||||||26-MAY-05
30670|Louisa Monzogranite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Paperbark Supersuite.||||||07-NOV-08
30670|Louisa Monzogranite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Paperbark Supersuite.|||Coarsely porphyritic syenogranite and monzogranite|
30670|Louisa Monzogranite|72437|6|Mentioned|p76-77|||||Paperbark Supersuite||||
35979|Lowendal Member|23379|5|Briefly described|p160 Fig2|||Of Flacourt Formation, Barrow Sub-basin.||||||30-NOV-06
35669|Lowes Sandstone|23142|5|Briefly described|p203 Fig.2|||||||||
35669|Lowes Sandstone|60625|6|Mentioned|p48 Fig.2|||Geological Province: Eastern Goldfields.||||||
35669|Lowes Sandstone|65834|6|Mentioned|p36|||Kanowna Belle gold mine, Boorara Domain, Kalgoorlie Terrane. Mine terminology.||||Overlies QED Rudite. Is intruded by Kanowna Belle Porphyry.|A spatially-restricted, highly altered feldspar-quartz sandstone.|
28700|Luluigui Formation|7433|6|Mentioned|p25 Fig.2. |||Canning Basin.||||||
28700|Luluigui Formation|12733|6|Mentioned|p565.|||Canning Basin. Contains oil-prone basal marine shales.||||||
28700|Luluigui Formation|22741|6|Mentioned|P24||Devonian|||||||
28700|Luluigui Formation|22764|4|Described|Table2, p11||Late Devonian|?700 m.||||||01-FEB-10
28700|Luluigui Formation|22765|6|Mentioned|P9||Devonian|||||||
28700|Luluigui Formation|22767|5|Briefly described|Table3 P18, P20||Late Devonian|||||||
28700|Luluigui Formation|22776|4|Described|Table.3|Late Devonian|Late Devonian|Ostracods, conodonts and palynomorphs in fossil assemblage.||||||
28700|Luluigui Formation|23722|5|Briefly described|p34|Early Carboniferous|Late Devonian|Geological Province: Canning Basin. Underlies the Gumhole Formation (Fairfield Group) in Napier 4.||||||01-FEB-10
28700|Luluigui Formation|24061|5|Briefly described|p180|||Geological Province:  Canning Basin.||||||
28700|Luluigui Formation|30110|6|Mentioned|p81|||See P83. U.Devonian - L.Carboniferous, Famennian - Tournaisian age.||||||
28700|Luluigui Formation|30595|5|Briefly described|p3|||||||||
28700|Luluigui Formation|32648|6|Mentioned|p32|||Famennian||||||
28700|Luluigui Formation|32865|4|Described|p476|||||||||
28700|Luluigui Formation|33518|6|Mentioned|p8|||||||||
28700|Luluigui Formation|33965|6|Mentioned|p13|||||||||
28700|Luluigui Formation|35120|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
28700|Luluigui Formation|36224|5|Briefly described|Map legend|Late Devonian|Late Devonian|Interbedded siltstone, shale, limestone, fine sandstone.||||||01-FEB-05
28700|Luluigui Formation|36634|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
28700|Luluigui Formation|36890|3|Fully described|p337|||||||||
28700|Luluigui Formation|38878|6|Mentioned|Map legend|Famennian|Famennian|||||||
28700|Luluigui Formation|40992|6|Mentioned|Fig.11|||||||||
28700|Luluigui Formation|41023|4|Described|p288|||||||||
28700|Luluigui Formation|41215|6|Mentioned|Fig.4|||||||||
28700|Luluigui Formation|41217|5|Briefly described|p310|||||||||
28700|Luluigui Formation|41730|6|Mentioned|Fig.3|||||||||
28700|Luluigui Formation|41839|6|Mentioned|p21|||||||||
28700|Luluigui Formation|42547|6|Mentioned|p92|||||||||
28700|Luluigui Formation|42814|6|Mentioned|p23|||||||||
28700|Luluigui Formation|42860|5|Briefly described|Fig.2|||||||||
28700|Luluigui Formation|43173|6|Mentioned|54||Late Devonian|||||||
28700|Luluigui Formation|43563|6|Mentioned|Fig.5,p10||Late Devonian|||||||
28700|Luluigui Formation|43656|6|Mentioned|Fig.2,p8|Famennian|Famennian|||||||
28700|Luluigui Formation|43932|6|Mentioned|p4|||||||||
28700|Luluigui Formation|44143|4|Described|p.439 Table 4-19, p442|Devonian|Devonian|Up to 1000m thick; siltstone, shale, limestone, and sandstone; marine. Conformably overlies Clanmeyer Siltstone. Type section between 1084m and 1909m in Frome Rocks 2 (MOUNT ANDERSON: 18 deg 15' 15" S, 123 deg 39' 35" E). Contains microfossils, conodonts and ostracods: Famennian.||||||23-NOV-17
28700|Luluigui Formation|45041|6|Mentioned|Fig.45|||U.Dev.||||||
28700|Luluigui Formation|45063|6|Mentioned|Fig. 9|||Devonian||||||
28700|Luluigui Formation|45133|6|Mentioned|p2|||See also Fig.2||||||
28700|Luluigui Formation|45143|6|Mentioned|p22|||||||||
28700|Luluigui Formation|45153|2|Defined|App.3-44|Famennian|Famennian|See also App.2-28||||||
28700|Luluigui Formation|45158|3|Fully described|p26|||||||||
28700|Luluigui Formation|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
28700|Luluigui Formation|48978|6|Mentioned|Fig.2|||||||||
28700|Luluigui Formation|64187|5|Briefly described|p320 Fig. 2|Famennian|Famennian|Underlain by Clanmeyer Formation, overlain unconformably by Laurel Formation. Siltstone, shale, limestone (marine). Geological Province: Canning Basin.||||||15-FEB-10
28700|Luluigui Formation|65301|5|Briefly described|p5 Fig. 4|Late Devonian|Late Devonian|Geological province: Canning Basin.||||||
28700|Luluigui Formation|65449|6|Mentioned|p6|Late Devonian|Late Devonian|||||||
28700|Luluigui Formation|68007|6|Mentioned|p4|Late Devonian|Late Devonian|Canning Basin.||||||25-FEB-20
28700|Luluigui Formation|68902|6|Mentioned|p9 fig 5|Carboniferous|Carboniferous|||||||
28700|Luluigui Formation|69182|6|Mentioned|Ch4 p30-p35, Ch4 p39|||Canning Basin. See also Ch4 p44-p45, Ch4 p90.||||||
28700|Luluigui Formation|69297|6|Mentioned|p337, p352, p354|Famennian|Famennian|Broome Platform of the Canning Basin. ||||Overlies the Clanmeyer Formation. Overlain by the Gumhole Formation.||
28700|Luluigui Formation|69312|6|Mentioned|p19, p30|Devonian|Devonian|Canning Basin. ||||Overlain by the Gumhole Formation. Overlies the Clanmeyer [Siltstone]. Equivalent to the Clanmeyer and Laurel Formations.||11-FEB-20
28700|Luluigui Formation|70492|6|Mentioned|p175|||Lennard Shelf, Canning Basin.||||Coeval with Fairfield Group.||
28700|Luluigui Formation|70774|5|Briefly described|p4|Mississippian|Late Devonian|Canning Basin.||||Overlain by the Fairfield Group.||10-FEB-20
28700|Luluigui Formation|72497|5|Briefly described|p3 Fig.2.|Famennian|Famennian|Shown as occuring in the Jurgurra and Barbwire Terraces and Broome Platform.||||Conformably underlies Fairfield Group and laterally equivalent to Babrongan Reef Complex.||
28700|Luluigui Formation|72499|5|Briefly described|p87 App.3.2.|Famennian|Famennian|Recorded ~1100 - 1900m in Frome Rocks 2 well.||||Overlies Clanmeyer Formation and unconformably underlies Grant Group.|Includes conodonts, ostracods and pelecypod fossils.|
28700|Luluigui Formation|72502|5|Briefly described|p3, p5|Upper Famennian|Upper Famennian|Lennard Shelf/Fitzroy Trough, Canning Basin. Only known from the subsurface. Authors indicate that this part of the succession needs revision. Druce and Radke (1979) and Edgell (2004) claim it is overlain by the Gumhole Formation in the Napier and Oscar Ranges.||||Possibly overlain by Gumhole Formation.|Includes fine-grained siliciclastic facies with minor carbonate.|
28700|Luluigui Formation|73117|6|Mentioned|p140|||||||Underlain by Clanmeyer Formation. Unconformably overlain by Grant Group and Noonkanbah Formation.||
35680|Lungkarta Formation|50085|5|Briefly described|p11 Fig. 6|Cambrian|Neoproterozoic|Age: ~540Ma. Geological Province: Officer Basin.||||||11-APR-08
35680|Lungkarta Formation|61023|5|Briefly described|p15 Fig. 8|Cambrian|Neoproterozoic|Geological Province: Officer Basin.||||||11-APR-08
35680|Lungkarta Formation|61732|5|Briefly described|p4 Fig. 3, p84, p89|Marinoan|Marinoan|This name replaces the previous (and now abandoned) "Babbagoola Formation" and "McFadden Formation equivalent". Geological Province: central Officer Basin.||||||07-FEB-11
35680|Lungkarta Formation|62453|3|Fully described|p5 Fig. 3, 22, 47|Ediacaran|Ediacaran|Geological Province: Officer Basin. Underlies: Table Hill Volcanics, Durba Sandstone. Overlies: Wahlgu Group. Sandstone, siltstone, mudstone, evaporites, conglomerate.||||||
35680|Lungkarta Formation|62987|5|Briefly described|p30|||Sandstone-dominated aeolian unit. Overlies the Wahlgu Group. Geological Province: Officer Basin.||||||25-JAN-07
35680|Lungkarta Formation|63022|5|Briefly described|p1014-1015|Neoproterozoic|Neoproterozoic|Of Disappointment Group. Geological Province: Officer Basin. In Supersequence 4. See also p1016 Fig. 2.||||||10-AUG-07
35680|Lungkarta Formation|64103|4|Described|p399 Fig. 2, p400 Fig. 3, p400-402|Ediacaran|Ediacaran|Formation is Fm in text. Overlain by Table Hill Vols; underlain by Wahlgu Fm. Geological Province: Officer Basin. Depositional env in present study is eolian dune, interdune. See p401-402 for detailed information. Eolian sandstone.||||||07-FEB-11
35680|Lungkarta Formation|64325|6|Mentioned|p85|||Of Grey et al (in prep.). Correlative of McFadden Formation.||||||26-AUG-08
35680|Lungkarta Formation|65363|4|Described|p1, p6 Fig.5,  p7, p19.|Neoproterozoic|Neoproterozoic|Officer Basin. Formerly 'Babbagoola beds' (Townson 1985) and 'McFadden Formation equivalent' (Apak and Moors 2000). The upper part was deposited subaqueously (fluvial or high-energy shallow-marine); the lower part mainly under eolian conditions. Age may extend into Early Cambrian. Porosity and permeability are briefly discussed. The eolian sandstone of this unit is remarkably similar to, and in the same relative stratigraphic position as, the McFadden Formation.|c.550 - 510 Ma.|||Disconformably overlies Wahlgu Formation. Is overlain unconformably by Paterson Formation and Table Hill Volcanics.|Reddish-brown, medium-grained, poorly to well sorted, well-rounded quartz-rich sandstone, minor mudstone intervals and polymict lithic-granule conglomerate increasing in abundance towards the base..|
35680|Lungkarta Formation|65364|5|Briefly described|p81|||Officer Basin.||||Overlain by Durba Sandstone; underlain by Wahlgu Formation.|Reddish brown sandstone and minor basal polymict conglomerate.|16-MAR-12
35680|Lungkarta Formation|65366|5|Briefly described|p19|Neoproterozoic |Neoproterozoic |Possibly Ediacaran||||||
35680|Lungkarta Formation|65371|5|Briefly described|p54 Fig. 1|||Disconformable on Wahlgu Formation. Conformably overlain by ?Durba Sandstone. Reddish brown sandstone, minor conglomerate stringers and siltstones. Eolian depositional environment||||||
35680|Lungkarta Formation|67195|5|Briefly described|p10 fig 6|Neoproterozoic|Neoproterozoic|Western Officer Basin.|||||Sandstone.|
35680|Lungkarta Formation|67454|5|Briefly described|p563. |Neoproterozoic|Neoproterozoic|Officer Basin.|c.600 - 540 Ma.|||Overlies Wahlgu Formation. Is overlain by Durba Sandstone.||
35680|Lungkarta Formation|68270|5|Briefly described|p678,683|Ediacaran|Ediacaran|Western Officer Basin. ||||Underlain disconformably by Wahlgu Formation.||
35680|Lungkarta Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|Officer Basin.||||||
35680|Lungkarta Formation|69091|5|Briefly described|p44|Ediacaran|Ediacaran|Present in Empress 1A and Vines 1, but cannot be differentiated from glaciogene units below on the YOM seismic section||||Is disconformably overlain by Table Hill Volcanics.|Aeolian sandstone.|
35680|Lungkarta Formation|69445|6|Mentioned|p30:5, 17|||Officer Basin.||||Is overlain conformably by Table Hill Volcanics.||12-JUL-16
35680|Lungkarta Formation|71618|6|Mentioned|p131|||Succession with significant aeolian influence, deposited in response to Paterson-Petermann Orogeny.||||||
35680|Lungkarta Formation|73392|6|Mentioned|p4||||||||Sampled from core of GSWA Vines 1 well.|
41591|Lyally Conglomerate|22496|5|Briefly described|p12|Early Cambrian|Early Cambrian|||||||
31964|Lyndon River Granite|24197|6|Mentioned|p71 Tb. 7.1|||Of the Minnie Creek Supersuite.||||||07-FEB-11
31964|Lyndon River Granite|50425|5|Briefly described|p1.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Province. Of the Minnie Creek Supersuite.||||||07-NOV-08
38795|Lyons Basalt|23926|6|Mentioned|p33 Fig. 15|||Geological Province: Yilgarn Craton.||||||
38795|Lyons Basalt|23931|6|Mentioned|p200 Fig.2|||Geological Province: Yilgarn Craton.||||||
38796|Lyons Dolerite|23926|6|Mentioned|p33 Fig. 15|||Geological Province: Yilgarn Craton.||||||
38796|Lyons Dolerite|23931|6|Mentioned|p200 Fig.2|||Geological Province: Yilgarn Craton.||||||
28702|Lyons Group|12466|5|Briefly described|p178.|Permian|Permian|Enderby Terrace, Dampier Sub-basin. No demonstrated hydrocarbon source potential.|||||Sandstones and claystones.|
28702|Lyons Group|12471|6|Mentioned|p475 Fig.2. |Early Permian|Late Carboniferous|Shelfal glaciomarine environments; mainly fine-grained. ||||Is overlain by Callytharra Formation.||
28702|Lyons Group|12729|5|Briefly described|p. 15, 20, 28, 32, Figs. 6, 16, 23.|Early Permian|Late Carboniferous|Deposition in a glacio-marine environment. Thick (increasing to the north). Gascoyne Platform. ||||?Unconformably overlies the Quail Formation.|Glacial siltstone and shale.|
28702|Lyons Group|12731|5|Briefly described|p590 Fig.2.|Early Permian|Late Carboniferous||||||Glacigene deposition.|
28702|Lyons Group|12733|5|Briefly described|p554 Fig.2.|Early Permian|Late Carboniferous|Stephanian-Asselian.||||Is overlain by Callytharra Formation.|Marine glacigene deposition.|
28702|Lyons Group|13615|3|Fully described|p3-4, p6-8, p12, p14-16, 17|Sakmarian|Late Carboniferous|Peedamullah Shelf. Mostly between 200-1000m thick, can be up to 3000m thick. Spores and Pollen zone provided. Intersected in numerous drillholes. Deposited in a marine shelf to lacustrine environment with pronounced glacial influence. The type section occurs in the North side of the Wyndham River; 25deg02'35"S 115deg42'20" E. See also p18, p27, p29-p30, p32-p34, p39, p41-p44, p49-p51, p54-p59, p63, p65-p67, p69, p76, p80, p83-p85, p103 App. 3,  p118, Plates 2, 3.|c. 305 Ma||May  Include the Callytharra Formation?|Unconformably overlies the Quail Formation. Unconformably overlain by the Kennedy Group.|Siliciclastic sandstone, siltstone, diamictite and conglomerate.|07-FEB-19
28702|Lyons Group|14228|5|Briefly described|p5 fig 2, p7-8, p10, p15, p17-19|Early Permian|Late Carboniferous|Mixed siliciclastic facies deposited in a glacially influenced marine environment. Up to 3km thick, deposition rate 30m/my.|||Harris Sandstone (at base).|Overlain by Callytharra Formation (conformably).|Mostly shale. Mass-flow diamictites, poorly sorted conglomerates, and common deformation structures attributed to downslope slumping|
28702|Lyons Group|22814|5|Briefly described|fig2|Early Permian|Carboniferous|||||||
28702|Lyons Group|22817|6|Mentioned|p2|||||||||
28702|Lyons Group|23174|5|Briefly described|Fig5p8|||||||||
28702|Lyons Group|23296|14|Not recorded|p55|||Age from plant fossils: Carboniferous or Permian.||||||
28702|Lyons Group|23297|14|Not recorded|not recorded|||marine fauna.||||||
28702|Lyons Group|23403|4|Described|p7|Late Permian|Middle Devonian|||||||
28702|Lyons Group|23525|4|Described|p31|Early Permian|Late Carboniferous|Formerly "Lyons Formation". Age: 320-270Ma. Geological Province: Carnarvon Basin.||||||11-APR-08
28702|Lyons Group|23527|5|Briefly described|Map Legend|Permian|Carboniferous|Southern Carnarvon Basin||||||
28702|Lyons Group|23569|4|Described|p4 Tb. 1|Early Permian|Early Permian|Formerly the Lyons Formation. Includes the Callytharra and Carandibby Formations.||||||28-OCT-09
28702|Lyons Group|23572|4|Described|p8 Fig. 6, p11|Asselian|Stephanian|Geological Province: Carnarvon Basin. Underlying Unit: Munabia Sandstone.||||||28-OCT-09
28702|Lyons Group|23574|5|Briefly described|Map Legend|Early Permian|Early Permian|Overlying unit Wooramel Group. Underlying unit Badgeradda Group.||||||
28702|Lyons Group|23576|5|Briefly described|Map Legend|Early Permian|Early Permian|Overlying unit Wooramel Group. Underlying unit Badgeradda Group.||||||
28702|Lyons Group|23577|5|Briefly described|Map Legend|Early Permian|Early Permian|Overlying unit Wooramel Group. Underlying unit Badgeradda Group.||||||
28702|Lyons Group|23620|5|Briefly described|p4 Fig. 4|Permian|Devonian|Marine and continental siltstone, shale, sandstone, and limestone: glacially influenced.||||||11-APR-08
28702|Lyons Group|23726|5|Briefly described|p37|Early Permian|Late Carboniferous|Geological Province: Carnarvon Basin.||||||
28702|Lyons Group|23815|4|Described|p278|Sakmarian|Sakmarian|Geological Province: Carnarvon Basin. Underlying unit: Harris Sandstone (unconformable). Overlying units: Callytharra Formation and Carrandibby Formation (both conformable). Max. thickness:1478 m. Richly fossiliferous.||||||28-OCT-09
28702|Lyons Group|23935|5|Briefly described|p11 Fig.7|Asselian|Stephanian|Equivalent of Nangetty Formation. Geological Province: Southern Carnarvon Basin.||||||27-JAN-05
28702|Lyons Group|23976|5|Briefly described|Map Legend|Permian|Devonian|||||||
28702|Lyons Group|23977|5|Briefly described|Map Legend|Permian|Devonian|||||||
28702|Lyons Group|23978|5|Briefly described|Map Legend|Permian|Devonian|||||||
28702|Lyons Group|24044|5|Briefly described|p541 Fig.2|Early Permian|Carboniferous|||||||
28702|Lyons Group|24059|5|Briefly described|p137|Permian|Permian|Geological Province: Carnarvon Basin.||||||
28702|Lyons Group|24114|5|Briefly described|p5 Fig.4|||Geological Province: Carnarvon Basin.||||||
28702|Lyons Group|24390|5|Briefly described|p19 Fig. 10|Permian|Carboniferous|Geological Province: Southern Carnarvon Basin.||||||
28702|Lyons Group|24410|5|Briefly described|p134 Fig. 79|Phanerozoic|Phanerozoic|Siltstone, shale, sandstone and limestone.||||||
28702|Lyons Group|29365|6|Mentioned|p181|||See also P185.||||||
28702|Lyons Group|29721|6|Mentioned|p181|||||||||
28702|Lyons Group|29889|6|Mentioned|p141|||||||||
28702|Lyons Group|30338|6|Mentioned|p101|||||||||
28702|Lyons Group|30340|6|Mentioned|p2533|||Lithology||||||
28702|Lyons Group|30341|4|Described|p145|||||||||
28702|Lyons Group|30545|6|Mentioned|Fig.2|||Sakmarian. See also P20||||||
28702|Lyons Group|31561|5|Briefly described|p32|||Sakmarian. Marine to lacustrian. See also P34.||||||
28702|Lyons Group|32094|6|Mentioned|p382|||||||||
28702|Lyons Group|32648|6|Mentioned|p32|||L. Perm.||||||
28702|Lyons Group|32789|5|Briefly described|p85|||Carboniferous - Permian boundary||||||
28702|Lyons Group|32868|6|Mentioned|p208|||||||||
28702|Lyons Group|32943|6|Mentioned|p86|||See also PP98,99,106. Bivalues||||||
28702|Lyons Group|32945|6|Mentioned|p73|||See also P87||||||
28702|Lyons Group|33386|6|Mentioned|Fig.7|||||||||
28702|Lyons Group|33450|6|Mentioned|p14|||||||||
28702|Lyons Group|33453|5|Briefly described|p70|||Sakmarian.||||||
28702|Lyons Group|33623|6|Mentioned|p54|||||||||
28702|Lyons Group|33701|6|Mentioned|p600|||See also Fig.1 Sakmarian.||||||
28702|Lyons Group|33711|6|Mentioned|Table 4|||||||||
28702|Lyons Group|33728|6|Mentioned|p56|||||||||
28702|Lyons Group|34008|6|Mentioned|p71|||L.Perm.||||||
28702|Lyons Group|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
28702|Lyons Group|34287|6|Mentioned|p121|||See also PP122, 146. Permian||||||
28702|Lyons Group|34532|6|Mentioned|p219|||Sakmarian.  See also PP220,223,etc.||||||
28702|Lyons Group|34570|6|Mentioned|p114|||||||||
28702|Lyons Group|34838|6|Mentioned|Fig.3|||||||||
28702|Lyons Group|34846|6|Mentioned|Fig.3|||||||||
28702|Lyons Group|35105|6|Mentioned|Fig.66|||||||||
28702|Lyons Group|35144|6|Mentioned|Fig.5|||||||||
28702|Lyons Group|35282|6|Mentioned|Fig.2|||||||||
28702|Lyons Group|35653|6|Mentioned|p1093|||Discussion of stratigraphy and basin development.||||||
28702|Lyons Group|35983|6|Mentioned|Table 27|||||||||
28702|Lyons Group|36020|6|Mentioned|p387|||See also P388.||||||
28702|Lyons Group|36253|6|Mentioned|p131|||||||||
28702|Lyons Group|36596|6|Mentioned|Text Fig.2|||||||||
28702|Lyons Group|36718|6|Mentioned|p459|||||||||
28702|Lyons Group|36794|6|Mentioned|p386|||||||||
28702|Lyons Group|36890|3|Fully described|p279|||Formerly Lyons Conglomerate.||||||11-APR-08
28702|Lyons Group|37295|6|Mentioned|Table 2|||||||||
28702|Lyons Group|37926|6|Mentioned|p500|||||||||
28702|Lyons Group|38217|4|Described|p269|||||||||
28702|Lyons Group|38482|6|Mentioned|Table 10|||||||||
28702|Lyons Group|38505|6|Mentioned|p1119|||||||||
28702|Lyons Group|38917|6|Mentioned|p158|||||||||
28702|Lyons Group|39223|6|Mentioned|p238|||||||||
28702|Lyons Group|39307|6|Mentioned|p44|||||||||
28702|Lyons Group|39427|4|Described|Table 1|||||||||
28702|Lyons Group|39865|6|Mentioned|p18|||||||||
28702|Lyons Group|40617|4|Described|p12|||||||||
28702|Lyons Group|40636|6|Mentioned|p44|||||||||
28702|Lyons Group|40992|6|Mentioned|Fig.8|||||||||
28702|Lyons Group|41044|6|Mentioned|p150|||||||||
28702|Lyons Group|41053|6|Mentioned|Fig.2|||Shown only as Lyons Gr.||||||
28702|Lyons Group|41172|6|Mentioned|p121|||||||||
28702|Lyons Group|41271|3|Fully described|p65|||Formerly "L. Conglomerate","L. Series","L. Formation".||||||11-APR-08
28702|Lyons Group|41315|6|Mentioned|p149|||||||||
28702|Lyons Group|41438|4|Described|p103|||||||||
28702|Lyons Group|41441|5|Briefly described|p151|||||||||
28702|Lyons Group|41443|4|Described|p163|||||||||
28702|Lyons Group|41444|6|Mentioned|Fig.4|||||||||
28702|Lyons Group|41446|6|Mentioned|Fig.17|||||||||
28702|Lyons Group|41637|6|Mentioned|p211|||||||||
28702|Lyons Group|41689|6|Mentioned|Table 1|||||||||
28702|Lyons Group|42000|6|Mentioned|p55|||||||||
28702|Lyons Group|42017|6|Mentioned|p9|||||||||
28702|Lyons Group|42116|4|Described|p27|||||||||
28702|Lyons Group|42392|5|Briefly described|p115|||||||||
28702|Lyons Group|42711|6|Mentioned|p19|||Geological province: Carnarvon Basin. Equivalent to Shotts Formation in the Collie Basin.||||||11-AUG-08
28702|Lyons Group|42994|6|Mentioned|p53|||||||||
28702|Lyons Group|43015|5|Briefly described|Table 1,p319|||||||||
28702|Lyons Group|43018|5|Briefly described|Table 1,p386|||||||||
28702|Lyons Group|43474|14|Not recorded|p25,26,55|||||||||
28702|Lyons Group|43495|6|Mentioned|5|||||||||
28702|Lyons Group|43566|6|Mentioned|p413|||||||||
28702|Lyons Group|43835|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
28702|Lyons Group|44040|14|Not recorded|p44,45|||||||||
28702|Lyons Group|44217|14|Not recorded|Fig.3|||||||||
28702|Lyons Group|44219|14|Not recorded|p31||Sakmarian|||||||
28702|Lyons Group|44344|14|Not recorded|p.6-9,10,20,24|||(G50-1). opp.4, map.||||||
28702|Lyons Group|44345|14|Not recorded|map legend||Sakmarian|||||||
28702|Lyons Group|44403|6|Mentioned|opp.p.6, Tb.1|||||||||
28702|Lyons Group|44479|2|Defined|Tb.1|||E/51-1. Correlates with Braeside Tillite of this Sheet.||||||
28702|Lyons Group|44532|4|Described|p.5,6,10,15, map|||Potential source & reservoir beds for petroleum. (G50-5).||||||
28702|Lyons Group|44533|5|Briefly described|map legend||Sakmarian|Sakmarian.||||||
28702|Lyons Group|44537|14|Not recorded|map legend||Sakmarian|||||||
28702|Lyons Group|44657|14|Not recorded|p.8|||||||||
28702|Lyons Group|44993|14|Not recorded|p.6|||Fig.3.||||||
28702|Lyons Group|44994|5|Briefly described|p11|||Sakmarian||||||
28702|Lyons Group|44998|14|Not recorded|p67,71|||||||||
28702|Lyons Group|45001|14|Not recorded|p7|Sakmarian|Sakmarian|||||||
28702|Lyons Group|45015|5|Briefly described|map legend,  p67|Sakmarian|Sakmarian|Unconformably overlies Williambury Formation, Badgeradda Group; disconformable on Munabia Sandstone.||||||01-JUN-06
28702|Lyons Group|45016|2|Defined|p.12,13,16,17-21||Sakmarian|Tb, p7,40,10,11,24-26,29-30,33,41,46,48-50,53-59,61-69,72,73,78,79,82,85,87,89,91,99,100,101,105,111,114,120,121,136,148,Fig.65,42. (F50-5,9,13,F49-12,16,G50-1,2,5,6,9,10,13).||||||
28702|Lyons Group|45142|6|Mentioned|p21|||||||||
28702|Lyons Group|46849|6|Mentioned|p195|||||||||
28702|Lyons Group|47041|6|Mentioned|p165|||||||||
28702|Lyons Group|48610|4|Described|p4,14,16,Pl.1,5,6|||(F50-13).||||||
28702|Lyons Group|48628|14|Not recorded|Figs.2,5, p.21.|||(F50-13/Wandagee).||||||
28702|Lyons Group|48823|4|Described|p27, map legend|Permian|Permian|Siltstone and sandstone with tillitic texture.||||||
28702|Lyons Group|48831|14|Not recorded|p.63,65,69,71-78|||||||||
28702|Lyons Group|48885|14|Not recorded|p.1,2,5,7-9,11,17||Early Permian|Lower Permian (Sakmarian-Artinskian). (G/50-6). pls.1,2.||||||
28702|Lyons Group|49644|5|Briefly described|Table|||||||||
28702|Lyons Group|49942|5|Briefly described|p4 Fig.3|Early Permian|Namurian|Geological Province: Gascoyne Platform.||||||
28702|Lyons Group|50026|5|Briefly described|p11|Phanerozoic|Phanerozoic|Geological Province: Coolgalalaya Sub-basin (Perth Basin).||||||11-APR-08
28702|Lyons Group|50084|5|Briefly described|p77||Middle Carboniferous|Glacially influenced sediments. Geological Province: Southern Carnarvon Basin.||||||07-FEB-11
28702|Lyons Group|50085|5|Briefly described|p19 Fig. 10|Late Carboniferous|Carboniferous|Geological Province: Southern Carnarvon Basin.||||||
28702|Lyons Group|60295|5|Briefly described|p130|Sakmarian||Geological Province: Carnarvon Basin.||||||
28702|Lyons Group|60296|5|Briefly described|p156 Fig.1|Sakmarian|Asselian|Geological Province: Carnarvon Basin.||||||11-APR-08
28702|Lyons Group|60331|5|Briefly described|p33 Fig.2|Sakmarian||Glacially influenced. Geological Province: Southern Carnarvon Basin.||||||
28702|Lyons Group|60384|6|Mentioned|p244, p243 Fig 2a|Early Permian|Carboniferous|Southern Carnarvon Basin. Mid-Carboniferous to Early Permian.||||||
28702|Lyons Group|60386|6|Mentioned|p291, 297|Sakmarian|Asselian|Glacially influenced. Post-rift transition phase following Alice Springs Orogeny. Deltaic - nearshore - shelf. ||||||
28702|Lyons Group|60725|5|Briefly described|p29 Fig.2, p30, p33 Fig.4, p36 Fig.6. |Early Permian|Carboniferous||||||Marine glacigene deposition.|
28702|Lyons Group|61023|5|Briefly described|p34 Fig. 14|Permian|Carboniferous|Geological Province: Southern Carnarvon Basin.||||||11-APR-08
28702|Lyons Group|61563|5|Briefly described|p578|Early Permian|Carboniferous|Age is Middle Carboniferous to Early Permian.  See also p579 fig. 3.||||||27-JAN-06
28702|Lyons Group|61958|5|Briefly described|Map sheets 1 and 2|Sakmarian|Sakmarian|Includes Austin Formation, Coyango Greywacke, Dumbardo Siltstone, Koomberan Greywacke, Mundarie Siltstone, Thambrong Formation and Weedarra Shale.||||||21-MAR-06
28702|Lyons Group|63469|5|Briefly described|map legend|Permian|Carboniferous|Includes; Harris Formation and Carrandibby Formation. Undivided; diamictite, sandstone and siltstone (locally calcareous), shale, boulber beds and lags; glacigene.||||||24-SEP-07
28702|Lyons Group|64502|6|Mentioned|p786|Early Permian|Late Carboniferous|Carnarvon Basin.||||||10-NOV-08
28702|Lyons Group|64580|4|Described|map legend|Permian|Carboniferous|Diamictite, sandstone and siltstone (locally calcareous), shale, boulder beds and lags; glacigene; includes Harris Sandstone (at base) and Carrandiby Formation (at top).||||||15-DEC-08
28702|Lyons Group|64630|5|Briefly described|p31 Fig.2, p33, 34, 35|Sakmarian|Bashkirian|Province: Southern Carnarvon Basin. Underlies the Callytharra Formation. Includes basal Harris Sandstone and uppermost Carrandibby Formation, otherwise undifferentiated. Palynology age: S. ybertii to P. confluens. Inferred glacial influence.||||||16-NOV-09
28702|Lyons Group|64972|5|Briefly described|p615, p615 Fig. 2, p616 Fig. 3|||Geological Province: Carnarvon Basin. Shale and pebbly siltstone. Also on p617 Fig. 4, p617 Fig. 5.||||||
28702|Lyons Group|64974|6|Mentioned|p147 Fig. 5|Sakmarian|Asselian|Geological Province: Carnarvon Basin.||||||24-JUN-09
28702|Lyons Group|64981|6|Mentioned|p670.|||Carnarvon Basin. Regional transgression at the base of this unit, and Nangetty and Mosswood Formations in Perth Basin, may be coeval with partial melting of extensive Carboniferous ice caps.||||||
28702|Lyons Group|65382|6|Mentioned|p717 App. 2|Serpukhovian|Serpukhovian|Carnarvon Basin. </= 322 Ma S. ybertii palynozone.||||||
28702|Lyons Group|65830|6|Mentioned|Plate 1|||Southern Carnarvon Basin.||||||
28702|Lyons Group|66189|6|Mentioned|p454, p455 Fig.2|Early Permian|Late Carboniferous|Glacial succession. Overlain by  Early Permian Callytharra Formation.||||||
28702|Lyons Group|66299|5|Briefly described|p85, pp250-251, p283.|Permian|Carboniferous|Sedimentary rocks.||||Unconformably overlies metamonzogranite of the Dalgaringa Supersuite, and Davey Well Granite and other units of Durlacher Supersuite.|Diamictite, sandstone and siltstone.|
28702|Lyons Group|66579|5|Briefly described|Map legend|Permian|Carboniferous|Southern Carnarvon Basin.|||Includes Carrandibby Formation and an unnamed unit of glacigene clastics.||Glacigene clastics.|
28702|Lyons Group|66949|6|Mentioned|p8|||Southern Carnarvon Basin. Includes distinct glacial features in subsurface (core) sections, coeval with Reeves Formation.||||||
28702|Lyons Group|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes fine-grained sandstone, cream coloured; light grey fine-grained sandstone with common flaser beds of dark grey siltstone; dark grey interbedded siltstone/fine-grained sandstone.|
28702|Lyons Group|67200|5|Briefly described|p7 fig 5, p47, p50, p55, p64, app 2 p5|Permian|Carboniferous|Thermal conductivity of 2.59 W/mK|||Includes Carrandibby Formation, Harris Sandstone||Crudely bedded tillite, fine grained sandstone and fine grained sandstone with flaser beds of siltstone. Interbedded siltstone and sandstone.|
28702|Lyons Group|67354|6|Mentioned|p106.|||Carnarvon Basin. The upper part is equivalent to Treachery Formation of the Bonaparte Basin: both contain G. confluens Oppel Zone, and evidence of ice-transported debris.||||||
28702|Lyons Group|67371|5|Briefly described|Map legend.|Permian|Carboniferous|Southern Carnarvon Basin.|||||Undivided: diamictite, sandstone and siltstone (locally calcareous), shale, and boulder beds and lags; glacigene.|
28702|Lyons Group|67373|5|Briefly described|Map legend.|Permian|Carboniferous|Southern Carnarvon Basin.|||Includes Harris Sandstone.||Undivided: diamictite, sandstone and siltstone (locally calcareous), shale, and boulder beds and lags; glacigene.|
28702|Lyons Group|67977|5|Briefly described|p480, p481 Fig. 2, p482 Fig. 3, p491|Sakmarian|Gzhelian|Features indicate deposition in glacio-marine environment: outsized clasts, diamictites and minor rhythmites (Eyles et al., 2003; Mory et al., 2008).||||Is conformably overlain by Callytharra Formation.|Includes sandstone.|18-SEP-14
28702|Lyons Group|69011|5|Briefly described|Map Legend|Permian|Carboniferous|Southern Carnarvon Basin.|||Includes the Harris Formation.|Overlain by the Callytharra Formation. Underlain by the Yindagindy Formation.|Includes undivided diamictite, sandstone and siltstone (locally calcareous), shale, and boulder beds and lags, glacigene; fine- to coarse-grained sandstone, minor siltstone and (near base) diamictite.|28-APR-14
28702|Lyons Group|69028|5|Briefly described|Map Legend|Permian|Carboniferous|Southern Carnarvon Basin.|||||Diamictite, sandstone and siltstone (locally calcareous), shale, and boulder beds and lags; glacigene.|06-MAY-14
28702|Lyons Group|69029|6|Mentioned|p326,328|Asselian|Namurian|Of onshore Carnarvon Basin.||||Overlain by Callytharra Formation. Underlain by Quail Formation.||
28702|Lyons Group|69166|5|Briefly described|geologyp_lut.csv|Sakmarian|Pennsylvanian||||||Undivided; diamictite, fine to coarse grained sandstone interbedded with siltstone and conglomerate  (locally calcareous), shale, and boulder beds and lags; glacigene|
28702|Lyons Group|69182|6|Mentioned|Ch2 p3, Ch3 p3, Ch3 p8|Middle Carboniferous|Middle Carboniferous|Perth Basin. Deposited in a glacially influenced marine environment. Porosities of sandstones in this group are generally too low for the storage of carbon dioxide. See also Ch3 p11, Ch3 p15, Ch3 p17-p20, Ch3 p23-p26, Ch3 p29, Ch3 p34-35, Ch3 p37, Ch3 p50, Ch3 p52-p52, Ch3 p54-p55, Ch3 p59, Ch3 p63, Ch3 p67-p68, Ch3 p71-p73. ||||Overlain by the Callytharra Formation, the Wooramel, Kennedy and Byro Groups.|Interbedded shale and sandstone.|
28702|Lyons Group|69297|5|Briefly described|p246, p249|Cisuralian|Pennsylvanian|Gascoyne Sub-basin of the Carnarvon Basin. Deposited in a glaciomarine environment. ||||Unconformably overlies the Quail Limestone. Unconformably overlain by the Woodleigh Formation or the Winning Group.|Shales and sandstones.|
28702|Lyons Group|69547|6|Mentioned|p182,193,195-198|Sakmarian|Asselian|Southern Carnarvon Basin. Glacially-influenced.||Includes Carrandibby Formation.||||
28702|Lyons Group|69558|6|Mentioned|p258 fig 419|Late Permian|Late Permian|||||Unconformably overlain by the Wogatti Sandstone. Faulted against the Learmonth Formation.||25-MAY-21
28702|Lyons Group|69583|5|Briefly described|p130,p133,p134 Fig.3,p135; Plates 2,3,4|Carboniferous|Carboniferous|Southern Carnarvon Basin. Seismic interpretation.|||||Undivided: diamictite, sandstone and siltstone (locally calcareous), shale, and boulder beds and lags; glacigene.|
28702|Lyons Group|70138|5|Briefly described|Map legend.|||Southern Carnarvon Basin.|||Harris Sandstone.|Overlies Yindagindy Formation.|Diamictite, sandstone and siltstone (locally calcareous), shale, and boulder beds and lags; glacigene.|
28702|Lyons Group|70774|5|Briefly described|p5 fig 3|Sakmarian|Asselian|Southern Carnarvon Basin.||||Overlain by the Carrandibby Formation and the Callytharra Formation.||
28702|Lyons Group|70795|4|Described|100k_geologyp_lut.csv|Sakmarian|Pennsylvanian|Also 100k_interpgeop_lut.csv|323-290 Ma||||Diamictite, sandstone and siltstone (locally calcareous), shale, and boulder beds and lags; glacigene.|
28702|Lyons Group|70814|6|Mentioned|p4|||||||||
28702|Lyons Group|70826|6|Mentioned|p6 tbl 3|Early Permian|Late Carboniferous|Southern Carnarvon Basin.||||||
28702|Lyons Group|71146|5|Briefly described|p6, p14 fig 9, p38|Sakmarian|Late Carboniferous|Southern Carnarvon Basin.||||Overlain by the Callytharra Formation.|Mudstone.|
28702|Lyons Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, greywacke, siltstone, tillite|
28702|Lyons Group|72034|5|Briefly described|500k_interpgeop16_lut|Sakmarian|Pennsylvanian|Byro Sub-basin; Gascoyne Platform; Glacigene rocks, Merlinleigh Sub-basin, Southern Carnarvon Basin.  Age from biostratigraphy.|||||Diamictite, sandstone and siltstone (locally calcareous), shale, and boulder beds and lags; glacigene.|
28702|Lyons Group|72505|5|Briefly described|p890|Asselian|Carboniferous|Southern Carnarvon Basin. Correlated with the P. Confluens and Microbaculispora tentula zones.||||Overlain by the Callytharra Formation.||
28702|Lyons Group|72910|4|Described|p3-5, p7-14, p16-21, p25-26, p30-35.|Sakmarian|Late Carboniferous|Thickness mostly >1000m max 3000m. Recognised in Byro and Merlinleigh Sub-basins and the Peedamullah Shelf of the Carnarvon Basin. See also p40, 41, 42.|||Includes Carrandibby Formation, Harris Sandstone.|Unconformably overlies older rock and conformably underlies Callytharra Formation. Laterally equivalent to Nangetty Formation and Holmwood Shale.|Varied, mostly siliciclastic, glacial features unifying theme of group. Includes dropstones in poorly sorted matrix at greater depth.|
28702|Lyons Group|73117|6|Mentioned|p15, p34-35|Asselian|Gzhelian|Southern Carnarvon Basin, Merlinleigh Sub-basin. Numerous macrofossil localities; none are particularly age diagnostic. Equivalent to Grant Group[?].||||Overlain by Callytharra Formation.||
28702|Lyons Group|73184|6|Mentioned|p201 Fig.12|Asselian|Asselian|Written as Lyons Gp.||||||
28702|Lyons Group|73623|5|Briefly described|p3-4, 16|||Merlinleigh Basin.||||Correlative of Nangetty Formation.|Includes units with diamictites alternating with shale formations (suggesting glaciation and ice retreat).|
36837|Lyre Creek Member|23570|5|Briefly described|p73|Archean|Archean|Of Hardey Formation.  Max. thickness: 1000m.   Geological Province: Pilbara Craton||||||07-NOV-08
36837|Lyre Creek Member|23575|5|Briefly described|Map Legend|Archean|Archean|Of Hardey Formation.||||||07-NOV-08
36837|Lyre Creek Member|23598|5|Briefly described|p13|||Of Hardey Formation. Geological Province: Pilbara Craton.||||||
36837|Lyre Creek Member|23794|5|Briefly described|Map Legend|Archean|Archean|Of Hardey Formation. Geological Province: Hamersley Basin.||||||07-NOV-08
36837|Lyre Creek Member|23936|5|Briefly described|p3|||Geological Province: Hamersley Province. Parent: Hardey Formation.||||||
36837|Lyre Creek Member|24023|5|Briefly described|p28|Archean|Archean|Of Hardey Formation, Fortescue Group.  Geological Province: Hamersley Basin.||||||07-NOV-08
36837|Lyre Creek Member|24024|5|Briefly described|Map Legend|Archean|Archean|Of the Cooya Pooya Dolerite, Fortescue Group. Geological Province: Hamersley Basin||||||07-NOV-08
36837|Lyre Creek Member|24352|5|Briefly described|Map legend|Archean|Archean|Parent: Hardey Formation.   Age: ~2760Ma.   Felsic tuff and agglomerate, and felsic to intermediate volcanoclastic sandstone and conglomerate.   Geological Province: Hamersley Basin||||||07-NOV-08
36837|Lyre Creek Member|24353|4|Described|p22, 23|Archean|Archean|Underlying Unit: Mount Roe Basalt. Parent: Hardey Formation. Geological Province: Pilbara Craton||||||07-NOV-08
36837|Lyre Creek Member|24541|6|Mentioned|p11 Tb.2|||Of the Hardey Formation.||||||
36837|Lyre Creek Member|24543|5|Briefly described|Map legend|Archean|Archean|Of the Hardey Formation (Fortescue Group).  Felsic volcaniclastic sandstone and tuff.||||||23-DEC-09
36837|Lyre Creek Member|50300|5|Briefly described|Map Legend|Archean|Archean|Of the Hardey Formation.  Geological Province: Hamersley Basin.  Underlies: Kylena Formation. Overlies: Coolajacka Member. Intruded by Cooya Pooya Dolerite.||||||07-NOV-08
36837|Lyre Creek Member|50382|5|Briefly described|Map Legend|Archean|Archean|Of Hardey Formation (Fortescue Group). Geological Province: Hamersley Basin, Pilbara Craton.||||||07-NOV-08
36837|Lyre Creek Member|63372|4|Described|Map Legend|Archean|Archean|Of the Hardey Formation. Geological Province: Hamersley Basin. Overlies: Coolajacka Member. Felsic agglomerate and felsic pyroclastic rocks.||||||07-NOV-08
36837|Lyre Creek Member|66217|6|Mentioned|p46.|||Fortescue Basin.||Unit in Hardey Formation.||||
36837|Lyre Creek Member|67201|4|Described|p29 Fig.15, p50|||In northern Pilbara Craton, Northern Fortescue Basin, Northwest Pilbara Sub-basin. The lower level of Cooya Pooya Dolerite (up to 150 m thick) was probably formed by trapping of basaltic magma beneath massive beds of Lyre Creek Member.||Hardey Formation||Cooya Pooya Dolerite intrudes Hardey Formation beneath Lyre Creek Member.|Felsic to intermediate volcanciclastic member.|24-NOV-16
36837|Lyre Creek Member|69299|3|Fully described|p6 Tb.1, p12,p14-19,p21, map, Figs.8-10|Archean|Archean|Previously Lyre Creek Agglomerate Member of Kriewaldt and Ryan (1967) and Williams (1968). West Pilbara. Age is assumed to be similar to felsic Bamboo Creek and Koongaling Volcanic Members (of Hardey Formation, northeast Pilbara sub-basin), dated at c. 2760 Ma (Pidgeon, 1984; Arndt et al., 1991). On COOYA POOYA, mapping indicates that Coolajacka Member stratigraphically underlies the Lyre Creek Member. Present interpretation suggests massive beds of Lyre Creek Member formed a barrier to upward intrusion of Cooya Pooya Dolerite's basaltic magma, and hence would explain laccolithic sill formed beneath Lyre Creek Member (see p18). Geol. Prov: Hamersley Basin, Pilbara Craton.|Assumed similar age to other members c. 2760 Ma|Of Hardey Formation.||Between Mount Roe Basalt and Kylena Formation (Kriewaldt and Ryan 1967); overlies Coolajacka Member; single rhyolite outcrop is overlain by Tumbiana Formation.|Andesitic to dacitic tuff and agglomerate, and volcaniclastic sandstone and conglomerate with acid to intermediate rock clasts; local abundant accretionary lapilli; single outcrop of rhyolite and rhyolitic tuff on COOYA POOYA.|01-JUL-14
36837|Lyre Creek Member|69301|5|Briefly described|p18 Fig.7|||Pilbara Craton. Fortescue Basin. Northwest Pilbara Sub-basin.||Hardey Formation||||
36837|Lyre Creek Member|69411|6|Mentioned|p290|Neoarchean|Neoarchean|Geological province: Pilbara Craton. ||Unit of Hardey Formation.||||
75711|M. australis Member|70066|5|Briefly described|Dampier: Fig.2; p2. Regional: Fig.6; p16|Barremian|Barremian|Dampier Sub-basin and Rankin Platform, Northern Carnarvon Basin. Also appears as M. australis Sandstone Member and M. australis sandstone. Marine to marginal marine glauconitic sandstones host commercial oil accumulations in the Barrow Sub-basin. Has potential for stratigraphic traps. Known informally as Stag Sandstone [although the ASUD has it as the informal Stag Sand].||Muderong Shale.||||
34608|M. australis Sandstone|22702|4|Described|p104,106,108-13||Barremian|Invalid and undefined name of Delfos & Boardman (1994) . Should be given a proper name.||||||
34608|M. australis Sandstone|24246|6|Mentioned|p18|||Informal - see Muderong Shale. Geological Province: Carnarvon Basin.||||||24-FEB-05
34608|M. australis Sandstone|44938|4|Described|p151, Fig.3, p149-15||Barremian|Invalid, should be given proper name.||||||
34608|M. australis Sandstone|62837|5|Briefly described|Table B|Early Cretaceous|Early Cretaceous|Geological Province: Dampier Sub-basin.||||||08-NOV-06
34608|M. australis Sandstone|63950|5|Briefly described|p336 Fig. 4|Barremian|Barremian|Of the Muderong Shale. Geological Province: northern Carnarvon Basin. Written as M.australis Sst.||||||27-MAY-08
34608|M. australis Sandstone|64973|3|Fully described|p503-512, p505 Fig. 3, p504 Fig. 2|Barremian|Barremian|Overlain by Windalia Sandstone. Geological Prov: Carnarvon Basin. Three depositional sequences included in the unit, A, B and C. Typically very fine to fine-grained, moderately to well-sorted glauconitic sandstone grading to greensand. On p506 Fig. 4.||||||21-AUG-12
34608|M. australis Sandstone|70064|6|Mentioned|Regional p9|||Browse Basin. Had indications of residual hydrocarbons in Braveheart 1 ST1.||||||12-JUL-16
30660|Mabel Downs Suite|23925|5|Briefly described|p222 Table 3|||Geological Province: Halls Creek Orogen.||||||
30660|Mabel Downs Suite|50437|6|Mentioned|p4.1|||Of the Sally Downs Supersuite. Geological Province: Kimberley Region.||||||
30660|Mabel Downs Suite|64722|6|Mentioned|p24|||Of Kimberley Craton.||||||
30660|Mabel Downs Suite|65359|6|Mentioned|p23|||Felsic Suite in the Kimberley region.||||||
30660|Mabel Downs Suite|68078|6|Mentioned|p23|||||||||
30660|Mabel Downs Suite|69099|5|Briefly described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Of Sally Downs Supersuite.|Includes Sally Downs Tonalite, McHale Granodiorite, Mabel Downs Tonalite.|||
30660|Mabel Downs Suite|69165|6|Mentioned|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||||Includes Sally Downs Tonalite, McHale Granite, Mabel Downs Tonalite|||
30660|Mabel Downs Suite|69634|5|Briefly described|100k_interpgeop_lut.csv||||||Includes Mabel Downs Tonalite, Sally Downs Tonalite.|||
30660|Mabel Downs Suite|70154|6|Mentioned|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1821-1832 Ma|Sally Downs Supersuite||||
30660|Mabel Downs Suite|70812|4|Described|p8, p13, p24-p25|Orosirian|Orosirian|Lamboo Province, most commonly in the Central Zone although units occur throughout the whole length of the province. Interpreted to have formed over a west or northwest dipping subduction zone in the Halls Creek orogeny. This unit was subsequently metamorphosed and deformed at amphibolite facies conditions. Mineralisation is described.|c. 1835-1805 Ma|Sally Downs Supersuite|||Hornblende and hornblende-biotite tonalite and quartz diorite.|
30660|Mabel Downs Suite|70851|5|Briefly described|p5|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province. This units geochemistry shows overlap between Archean high-Al tonalite-trondhjemite-granodiorite suites and Phanerozoic adakites.||Sally Downs Supersuite|||Granitic rocks.|
30660|Mabel Downs Suite|71113|5|Briefly described|p101|Orosirian|Orosirian|Geological province: Central Zone, Lamboo Province, Halls Creek Orogen. Formed in a subduction zone setting.|>1820 Ma|Unit of Sally Downs Supersuite.||||
30660|Mabel Downs Suite|71140|6|Mentioned|p101|Orosirian|Orosirian|Lamboo Province, Halls Creek Orogen. Probably formed in a subduction zone setting.|1820 Ma.|Sally Downs Supersuite.||||
30660|Mabel Downs Suite|71267|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma).||Unit of Sally Downs Supersuite.|Includes Mabel Downs Tonalite, Sally Downs Tonalite, McHale Granodiorite.|||
31784|Mabel Downs Tonalite|22537|6|Mentioned|34, 36, 37|Proterozoic|Proterozoic|||||||
31784|Mabel Downs Tonalite|22547|3|Fully described|p17|Orosirian|Orosirian|Of the Sally Downs supersuite. Age: 1832 +/- 3 Ma. Formerly Mabel Downs Granodiorite (1969)||||||14-NOV-06
31784|Mabel Downs Tonalite|22754|5|Briefly described|p7|||Of the Sally Downs supersuite.  Age: 1832Ma.||||||
31784|Mabel Downs Tonalite|22783|6|Mentioned|p8|||||||||
31784|Mabel Downs Tonalite|23323|5|Briefly described|p454, p457 Fig. 4|Orosirian|Orosirian|Age: 1832 +/- 3 Ma.||||||07-FEB-07
31784|Mabel Downs Tonalite|23568|5|Briefly described|p2776|Paleoproterozoic|Paleoproterozoic|Age: ~1835 to 1830 Ma.||||||07-NOV-08
31784|Mabel Downs Tonalite|23751|4|Described|p17|Orosirian|Orosirian|Previously named Mabel Downs Granodiorite and Mabel Downs Granitoid Suite. Age: c.1830 Ma (SHRIMP U-Pb zircon). Of Mabel Downs suite.||||||
31784|Mabel Downs Tonalite|23925|5|Briefly described|p220|Orosirian|Orosirian|Age: 1832 +/- 3 Ma. Geological Province: Halls Creek Orogen.  Of the Mabel Downs Suite.||||||
31784|Mabel Downs Tonalite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs Supersuite. Age: 1825Ma. Geological province: Kimberley Province.||||||07-FEB-11
31784|Mabel Downs Tonalite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  In the Bow River batholith.  Age: 1835-1805Ma.||||||07-NOV-08
31784|Mabel Downs Tonalite|43853|5|Briefly described|Map Legend||Proterozoic|||||||
31784|Mabel Downs Tonalite|43854|5|Briefly described|Map Legend||Proterozoic|||||||
31784|Mabel Downs Tonalite|43855|5|Briefly described|Map Legend||Proterozoic|||||||
31784|Mabel Downs Tonalite|44230|5|Briefly described|Map Legend||Proterozoic|||||||
31784|Mabel Downs Tonalite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31784|Mabel Downs Tonalite|50437|5|Briefly described|p1.6, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Mabel Downs Suite (Sally Downs Supersuite). Age: 1821 +/- 4Ma (Shrimp).||||||07-NOV-08
31784|Mabel Downs Tonalite|60533|5|Briefly described|p592, 593 Fig. 2, 594, 596|Paleoproterozoic|Paleoproterozoic|Geological Province: Halls Creek Orogen. Age: 1835-1825Ma.||||||07-NOV-08
31784|Mabel Downs Tonalite|63866|5|Briefly described|p132|Orosirian|Orosirian|Central Zone, Halls Creek Orogen. Emplacement of this unit is interpreted as synchronous with the development of the northeast trending Ord River Shear Zone.|c. 1837-1827 Ma|Sally Downs Supersuite||||
31784|Mabel Downs Tonalite|65413|6|Mentioned|p104.|Paleoproterozoic|Paleoproterozoic|West of Halls Creek Fault. Locally strongly deformed, but little evidence of hydrothermal activity; contrasts with coeval McHale Granodiorite.||||||
31784|Mabel Downs Tonalite|66845|4|Described|p537 Fig.3, p539 Tb.1, p541, p542|||Unambiguous magmatic zircon crystallisation ages. Dyke analysed intruded Tickalara Metamorphics.|1832+/-3 Ma and 1829+/-4 Ma (dyke), SHRIMP U-Pb|||intrudes Tickalara Metamorphics|Foliated hornblende-biotite tonalite, dyke (foliated biotite tonalite).|31-JUL-15
31784|Mabel Downs Tonalite|66846|5|Briefly described|p558 Table 4|Orosirian|Orosirian|Age probably from U-Pb SHRIMP dating of zircon (see p547). |~1832 Ma|Of Mabel Downs suite.||||
31784|Mabel Downs Tonalite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Data from OZCHRON1. Comment: 'This is an excellent crystallisation age for the Mabel Downs Granodiorite. This is a maximum age for the D3 deformation.'|crystallisation age 1832+/-3 Ma U/Pb SHRIMP|Mabel Downs Suite|||Medium- to fine-grained, foliated, hornblende-biotite metatonalite; abundant flattened inclusions of mafic rock.|31-JUL-15
31784|Mabel Downs Tonalite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv. |1821-1832 Ma|Mabel Downs Suite|||Medium to fine grained, foliated, hornblende-biotite metatonalite; abundant flattened inclusions of mafic rock.|
31784|Mabel Downs Tonalite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2.|1832-1829 Ma (Isotopic)|Unit of Mabel Downs Suite.|||Medium- to fine-grained, foliated, hornblende-biotite metatonalite; abundant flattened inclusions of mafic rock|
31784|Mabel Downs Tonalite|70154|5|Briefly described|GA_geochron.csv|Paleoproterozoic|Paleoproterozoic|See also 100k_interpgeop_lut.csv|1829-1832 Ma|Mabel Downs Suite|||Medium-fine grained, foliated, hornblende biotite metatonalite, abundant flattened inclusions of mafic rock.|
31784|Mabel Downs Tonalite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1832+\-3 Ma to 1829+\-4 Ma (isotopic)|Unit of Mabel Downs Suite.|||Medium- to fine-grained, foliated, hornblende-biotite metatonalite; abundant flattened inclusions of mafic rock|
31784|Mabel Downs Tonalite|71397|5|Briefly described|p8,42|Orosirian|Orosirian|Geological province: Central Zone, Lamboo Province, Halls Creek Orogen. Emplaced during Halls Creek Orogeny.|1832+\-5 Ma; 1829+\-4 Ma|Unit of Sally Downs Supersuite.||||
31784|Mabel Downs Tonalite|71873|5|Briefly described|p442|Orosirian|Orosirian|Geological province: Lamboo Province. Emplacement constrains the timing of deformation and metamorphism in the Lamboo Province associated with 1835-1800 Ma Halls Creek Orogeny.|1835 Ma|||||
31784|Mabel Downs Tonalite|72437|5|Briefly described|p10, p96-98|Palaeoproterozoic|Palaeoproterozoic|Includes rocks previously called the Ord River Tonalite by Ogasawara (1988) as they can be directly traced into this unit. Previously the Mabel Downs Granitoid of Ogasawara (1988).|c. 1835-1815 Ma|Mabel Downs suite|||Tonalite.|
77863|MacPhersons Tonalite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2699 +/- 6 Ma (isotopic).||||Fine-grained, plagioclase biotite tonalite to granodiorite; biotite-quartz-rich inclusions; massive to foliated; metamorphosed.|
77863|MacPhersons Tonalite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2699+\-6 Ma||||Fine-grained, plagioclase biotite tonalite to granodiorite; biotite--quartz-rich inclusions; massive to foliated; metamorphosed|
40311|Macedon Sandstone|24390|5|Briefly described|p25 Table 6|||Geological Province: Northern Carnarvon Basin.||||||
40311|Macedon Sandstone|50085|5|Briefly described|p24 Tb. 6|Late Jurassic|Late Jurassic|Geological Province: Northern Carnarvon Basin (Exmouth Sub-basin).||||||
40311|Macedon Sandstone|61555|6|Mentioned|p234|||BHP Billiton nomenclature. Replaced by [invalid] Macedon Member.||||||
40311|Macedon Sandstone|69689|6|Mentioned|p16|Jurassic|Jurassic|Northern Carnarvon Basin.||||||
22234|Mad Gap Monzogranite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.||||||07-NOV-08
22234|Mad Gap Monzogranite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1850Ma. Geological province: Kimberley Province (East).||||||07-FEB-11
22234|Mad Gap Monzogranite|50437|5|Briefly described|p1.6, 3.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite.||||||07-NOV-08
22234|Mad Gap Monzogranite|72437|5|Briefly described|p79|||Lamboo Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Monzogranite, hornblende-biotite granodiorite.|
35002|Maddina Formation|23046|6|Mentioned|182|||Parent Fortescue Group||||||
35002|Maddina Formation|23484|5|Briefly described|p29|Archean|Archean|Age: 2717 +/- 2Ma.||||||07-NOV-08
35002|Maddina Formation|23570|4|Described|p16, p236 App.1|Archean|Archean|Text suggests that name replaces Maddina Basalt; however both names are used interchangeably throughout text.  Maddina Formation in this pub. refers to combined Maddina Basalt, Kuruna Siltstone and Nymerina Basalt of Hickman & Lipple (1976).||||||01-JUL-14
35002|Maddina Formation|23575|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Overlying unit Jeerinah Formation. Underlying unit Tumbiana Formation.||||||07-NOV-08
35002|Maddina Formation|23583|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Underlain by Tumbiana Formation. Geological Province Hamersley Basin.||||||07-NOV-08
35002|Maddina Formation|23585|4|Described|p17|Archean|Archean|Previously Maddina Basalt. Of Fortescue Group. Overlain by Jeerinah Formation. Underlain by Tumbiana Formation. Hamersley Basin. Max. thickness: 1000 m.||||||07-NOV-08
35002|Maddina Formation|23598|4|Described|p13|Archean|Archean|Of Fortescue Group. Underlain by Tumbiana Formation. Geological Province: Pilbara Craton.||||||07-NOV-08
35002|Maddina Formation|24025|5|Briefly described|p14|Archean|Archean|Of Fortescue Group.  Geological Province: Hamersley Basin.||||||07-NOV-08
35002|Maddina Formation|24110|5|Briefly described|Plate 1|Archean|Archean|Parent: Fortescue Group. Geological Province: Hamersley Basin||||||07-NOV-08
35002|Maddina Formation|24352|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group. Massive, vesicular and amygdaloidal basalt and basaltic andesite, with minor andesite, dacite and rhyolite.  Age: ~2717Ma.  Geological Province: Hamersley Basin||||||07-NOV-08
35002|Maddina Formation|24353|3|Fully described|p1, p9 Fig.5, p11 Tb.2|Archean|Archean|Of the Fortescue Group. Conformably underlain by Tumbiana Formation. Age: c.2717Ma. Max Thickness: 1100m. Geological Province: Hamersley Basin.||||||07-NOV-08
35002|Maddina Formation|24533|5|Briefly described|p11, 5 Table 2|Archean|Archean|Of the Fortescue Group. Includes the Kuruna Member. Consists of massive, vesicular and amygdaloidal basalt, and basaltic andesite. Age: 2717 +/- 2Ma (dacite).||||||07-NOV-08
35002|Maddina Formation|24534|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group (Mount Bruce Supergroup).  Massive, vesicular and amygdaloidal basalt and basaltic andesite.  Geological Province: Hamersley Basin.||||||07-NOV-08
35002|Maddina Formation|24541|3|Fully described|p1, p11 Tb.2, p51|Paleoproterozoic|Neoarchean|Of the Fortescue Group. Age: c. 2717 Ma. Conformably overlies the Tumbiana Formation. Maximum Thickness: 700m.||||||23-DEC-09
35002|Maddina Formation|24543|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group (Mount Bruce Supergroup).  Age: c.2717Ma.  Basalt and basaltic andesite; minor andesite, dacite and rhyolite.||||||07-NOV-08
35002|Maddina Formation|24554|5|Briefly described|p5, p13|||Of the Fortescue Group. Geological Province: Hamersley Basin, Pilbara Craton.||||||
35002|Maddina Formation|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Of the Fortescue Group. Massive to vesicular basalt and agglomerate.||||||07-FEB-11
35002|Maddina Formation|50146|5|Briefly described|Map Legend|Archean|Archean|Of the Fortescue Group. Age: c. 2717 Ma. Geological Province: Hamersley Basin. Massive, vesicular, and amygdaloidal basalt and basaltic andesite.||||||07-NOV-08
35002|Maddina Formation|50189|4|Described|p22-23, 31|Archean|Archean|Of the Fortescue Group. Supersedes the Maddina Basalt. Disconformably overlain by the Jeerinah Formation. Area divided between Nymerina and Maddina Basalts and Kuruna Siltstone now remapped as Maddina Formation. Max. Thickness: 600m.||||||07-NOV-08
35002|Maddina Formation|50287|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group (Mount Bruce Supergroup). Geological Province: Hamersley Basin.||||||07-NOV-08
35002|Maddina Formation|50300|5|Briefly described|Map Legend|Archean|Archean|Of the Fortescue Group.  Geological Province: Hamersley Basin.  Age: 2717Ma. Overlies: Tumbiana Formation.||||||07-NOV-08
35002|Maddina Formation|50382|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Geological Province: Hamersley Basin, Pilbara Craton. Age: c. 2717 Ma||||||07-NOV-08
35002|Maddina Formation|50544|4|Described|p49-50, p44 Fig. 8|Archean|Archean|Supersedes Maddina Basalt.  Contains the Kuruna Member, an important horizon marker.  Thick, massive, amygdaloidal and vesicular basalt and andesite.  Conformably overlies the Tumbiana Formation.  Max. thickness: 1000m.  Age: c.2717Ma.  See also p15 Tb.1.||||||07-NOV-08
35002|Maddina Formation|50555|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group (Mount Bruce Supergroup).  Massive, vesicular and amygdaloidal basalt and andesite, with silicified flowtops.  Overlies Tumbiana Formation; underlies Jeerinah Formation.  Age: c.2717Ma.  Geological Province: Hamersley Basin.||||||07-NOV-08
35002|Maddina Formation|60373|4|Described|p145 Tb. 1, p150 Tb. 2|Archean|Archean|Of Fortescue Group. Overlain by Jeerinah Formation, underlain by Tumbiana Formation. Age: 2717+/-2Ma (SHRIMP). Dacite||||||01-JUL-14
35002|Maddina Formation|60429|4|Described|p20 Fig. 5, p21, p22-23|Archean|Archean|Of Fortescue Gp. Disconformably overlain by Jeerinah Fm; overlies Tumbiana Fm. Max. thickness: 600m. Contains all rocks previously above Tunbiana Formation, including Nymerina Basalt + Maddina Basalt, and Kuruna Siltstone (now downgraded to Kuruna Mbr).||||||07-FEB-11
35002|Maddina Formation|60635|6|Mentioned|p51 Fig. 2.2A|||||||||
35002|Maddina Formation|61254|5|Briefly described|p255-273|Neoarchean|Neoarchean|Lithology described in detail.|||Includes Kuruna Siltstone Member.|Unconformably overlies Tumbiana Formation. Is overlain by Jeerinah Formation.|Consists of mafic tuffaceous mudstones and sandstones and basalt lavas.|24-APR-20
35002|Maddina Formation|61265|4|Described|p43, p46-47 Fig.2|Archean|Archean|Supersedes the Maddina Basalt. Of the Fortescue Group. Age: 2717+/-2 Ma. Basalt, andesite, rhyolite and dacite. Max. thickness: ~740m. Geological Province: Pilbara Craton.||||||07-NOV-08
35002|Maddina Formation|61266|5|Briefly described|p58 tb.1|Archean|Archean|Of the Fortescue Group. Massive to vesicular basalt and agglomerate. Geological Province: Pilbara Craton.||||||07-NOV-08
35002|Maddina Formation|61268|5|Briefly described|p79, p81 Tb.1|||Of the Fortescue Group. Conformably overlies the Tumbiana Formation. Max. thickness: 700m. Massive to amygdaloidal basaltic flows and breccia, andsesite, dacite and rhyolite. See also p80 Fig.2, p83 Fig.4||||||
35002|Maddina Formation|62576|5|Briefly described|p619|Archean|Archean|Of the Fortescue Group. Overlain by Jeerinah Formation. Age: ca 2715Ma. Geological Province: Pilbara Craton. Tuffaceous and mafic volcanic rocks.||||||07-NOV-08
35002|Maddina Formation|63367|5|Briefly described|p230, p231 Fig.1, p236, p246. |Neoarchean|Neoarchean|Trace elements and REE + Y data discussed in detail.|2.72 Ga|Unit in Fortescue Group.|Includes Kuruna Member.|Equivalent to Bunjinah Formation.|Basalts and tuffaceous rocks.|
35002|Maddina Formation|63372|4|Described|Map Legend|Archean|Archean|Of the Fortescue Group. Geological Province: Hamersley Basin. Age: 2717Ma. Underlies Woodiana Member, Jeerinah Formation. Overlies Tumbiana Formation. Massive, vesicular and amygdaloidal basalt and basaltic andesite.||||||07-NOV-08
35002|Maddina Formation|63417|5|Briefly described|Map legend|Archean|Archean|Of Fortescue Group (Mount Bruce Supergroup). Age: 2718-2713Ma. Geological Province: Fortescue Basin. Massive, amygdaloidal or vesicular basalt and basaltic andesite; local komatiitic basalt, dacite and rhyolite.||||||07-NOV-08
35002|Maddina Formation|63854|5|Briefly described|p233, |Neoarchean|Neoarchean||ca.2717 Ma|Of the Fortescue Group.||||
35002|Maddina Formation|64580|4|Described|map legend||Neoarchean|Of Fortescue Group. Massive, amygdaloidal, or vesicular basalt and basaltic andesite; local komatiitic basalt, dacite and rhyolite.||||||15-DEC-08
35002|Maddina Formation|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Age: c. 2717Ma. Geological Province: Pilbara Craton. Massive, vesicular, and amygdaloidal basalt and andesite, with silicified flow tops.||||||07-FEB-11
35002|Maddina Formation|64654|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Includes Kuruna Member.  Age: 2718Ma - 2713Ma. Geological Province: Pilbara Craton (Hamersley Basin). Basalt; massive, fine grained, vesicular, and doleritic; thick flows and/or sills, to thin flows; local very coarse gas cavities.||||||17-NOV-08
35002|Maddina Formation|64656|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Age: 2718-2713Ma. Geological Province: Hamersley Basin. Basalt and minor andesite, dacite, and dolerite sills.||||||26-NOV-08
35002|Maddina Formation|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Includes Kuruna Member. Age: 2718-2713Ma.  Geological Province: Hamersley Basin. Basalt; massive fine grained, vesicular, and doleritic; thick flows; local very coarse gas cavities filled with quartz.||||||
35002|Maddina Formation|65008|5|Briefly described|p41, p7, p8 Fig.5, p15 Tb.1, p21-24|Neoarchean|Neoarchean|Hamersley Basin. A U-Pb zircon date of 2717 +/- 2 Ma (Nelson, 1998, p.133-135) was obtained from a massive, plagioclase-phyric dacite unit in the lower part of this formation.|2717 +/- 2 Ma|Of the Fortescue Group|||Consists of subaerial basalt flows, pillow lavas, fine- to coarse-grained mafic volcaniclastic rocks, and subordinate dacite, rhyolite, stromatolitic carbonate, and quartz sandstone.|
35002|Maddina Formation|65724|5|Briefly described|map legend|Neoarchaean|Neoarchaean|Of Fortescue Group. Includes Karuna Member. Underlies Jeerinah Formation. Basalt. Age: 2718-2713 Ma (geochronology: T. S. Blake et al 2004; D. R. Nelson 1998). Geol. Prov: Hamersley Basin, Pilbara Craton.||||||
35002|Maddina Formation|65726|5|Briefly described|Map legend|Archean|Archean|Hamersley Basin, Pilbara Craton.|c.2717 Ma (Nelson 1998).|Of Fortescue Group. |Includes Kuruna Member.||Massive, vesicular, and amygdaloidal basalt and andesite, with silicified flow tops.|
35002|Maddina Formation|65727|5|Briefly described|Map legend|Neoarchean|Neoarchean|Fortescue Basin.|2718 - 2713 Ma (Arndt et al. 1991).|Of Fortescue Group. |Includes Kuruna Member.||Massive, vesicular or amygdaloidal basalt and basaltic andesite; local komatiitic basalt, dacite and rhyolite.|
35002|Maddina Formation|65825|4|Described|p4, p7 Fig.4,  p22, p23. |Archean|Archean|Encompasses the former Nymerina Basalt, Maddina Basalt, and Kuruna Siltstone (MacLeod and de la Hunty 1966; Hickman 1983). A large dolerite sill intrudes along the contact with Jeerinah Formation.|2717 +/- 2 Ma (Nelson 1998).|Unit in Fortescue Group.||Conformably overlies Tumbiana Formation.|Dominated by locally vesicular or plagioclase-phyric mafic rocks: komatiitic basalt, and basaltic andesite and andesite with minor basalt; minor silicified siltstone and chert, siltstone and tuffaceous siltstone, locally with accretionary lapilli.|
35002|Maddina Formation|65827|3|Fully described|Tb.3 p12, p33 Fig.6, p39, p40|Neoarchean|Neoarchean|Kojan and Hickman (1988). Of Fortescue Group. Formerly Maddina Basalt (MacLeod and de la Hunty, 1966), Kuruna Siltstone and Nymerina Basalt. Includes Kuruna Member. Conformably overlies Tumbiana Formation;  shown equivalent to Mount Jope Supersequence(2). Subaerial fissure eruptions of basalt and andesite; intruded by dolerite sills. 2718-2713 Ma.||||||
35002|Maddina Formation|65828|5|Briefly described|Map legend|Archean|Archean||c.2717 Ma (Nelson 1998).|Unit in Fortescue Group.|Includes Kuruna Member.|Overlies Tumbiana Formation. Is overlain by Jeerinah Formation.|Basaltic andesite and andesite; massive to amygdaloidal basalt; komatiitic basalt; chert, includes silicified siltstone.|
35002|Maddina Formation|65829|3|Fully described|p7 Fig.3, p10, pp20-22, p32.|Neoarchean|Neoarchean|Formerly Maddina Basalt (MacLeod and de la Hunty 1966). Thickness c.1000 m. Subaerial fissure eruptions of basalt and andesite lavas. Some exposures of uppermost parts are ferruginised, suggesting weathering prior to deposition of overlying Jeerinah Formation. Local occurrences of overlying low, calcrete mesas. Hosts a probable meteorite impact site; a crater 27 m by 36 m is similar to the Dalgaranga crater but did not reveal any recognisable meteoric material.|2718 - 2713 Ma.|Unit in Fortescue Group.|Includes Kuruna Member.|Overlies conformably Tumbiana Formation. Is faulted against the Kylena Formation. Is overlain by Jeerinah Formation.|Stacked, massive, amygdaloidal and vesicular, fine- to coarse-grained, scoria-topped basalt flows; intercalated with comagmatic, medium- to coarse-grained dolerite sills and local thin tuffaceous volcaniclastic horizons; local columnar jointing.|
35002|Maddina Formation|66108|5|Briefly described|Map legend|Neoarchean|Neoarchean|Unit in Fortescue Group. 2718-2713 Ma. Massive, amygdaloidal, or vesicular basalt and basaltic andesite; local komatiitic basalt, dacite and rhyolite. Includes Kuruna Member.||||||
35002|Maddina Formation|66217|5|Briefly described|p45.|||Fortescue Basin.||Unit in Fortescue Group.|||Subaerial basaltic flows.|
35002|Maddina Formation|66685|5|Briefly described|p217 Fig.2; p218 |Archean|Archean|U-Pb zircon ages, Blake et al. (2004). A rhyolite has a zircon U-Pb age of 2717 +/- 2 Ma (Nelson, 1998).|2718 +/- 3 Ma - 2715 +/- 2 Ma.|Fortescue Group|Kuruna Member|Underlies the Jeerinah Formation, overlies the Tumbiana Formation.|Includes basalt, sandstone and stromatolites.|
35002|Maddina Formation|67183|5|Briefly described|p645 Tb.1|Archean|Archean|Formerly Maddina Basalt (see also p643, p651, p659, p660, p664-5, p671). Present in the Southern Pilbara and Oakover Basin.||Fortescue Group||Conformably underlies the Jeerinah Formation.||
35002|Maddina Formation|67201|4|Described|p28-30, p51|||In northern Pilbara Craton, Fortescue Basin. Boundary with overlying Jeerinah Formation does mark a significant change from volcanism to predominantly sedimentary deposition.||Fortescue Group|Kuruna Member|Overlies Tumbiana Formation apparently conformably, locally unconformably. Is conformably overlain by Woodiana Member (Jeerinah Formation). Equivalent to Bunjinah Formation.|Ultramafic-mafic-felsic volcanic cycles including komatiitic basalt, basalt, andesite, dacite and local rhyolite.|24-NOV-16
35002|Maddina Formation|67202|5|Briefly described|p125, p258|Archean|Archean|See also Maddina Basalt (p51-52).||Fortescue Group.||Overlies Tumbiana Formation. Is overlain by Jeerinah Formation.|Massive amygdaloidal, or vesicular basalt and basaltic andesite; local komatiitic basalt, dacite and rhyolite.|
35002|Maddina Formation|67229|5|Briefly described|p4-5, p7, p9-10|Neoarchean|Neoarchean|U-Pb zircon age by Nelson (1998); Kojan and Hickman (1998).|2717 +/- 2 Ma.|||Conformably overlies Tumbiana Formation.|Includes basalt.|
35002|Maddina Formation|68035|5|Briefly described|p292 Fig 6|Neoarchean|Neoarchean|Fortescue Basin. |2718 - 2713|Fortescue Group||Overlies Tumbiana Formation, Overlain by Jerrinah Formation.|Basalt.|
35002|Maddina Formation|68056|5|Briefly described|p170-171, 176-177, 184-185, 188, 190|Archean|Archean|Pilbara Craton. Fe, C isotope data and pyrite shapes tabulated.|c.2716 Ma.|Fortescue Group.|Kuruna Member.|Unconformably overlies the Meentheena Member (Tumbiana Formation). Is overlain unconformably by Woodiana Sandstone Member (Jeerinah Formation).|Basaltic and sedimentary rocks.|
35002|Maddina Formation|68101|6|Mentioned|p1, p6|||||Fortescue Group||Overlies Tumbiana Formation, unconformably overlain by Jeerinah Formation||
35002|Maddina Formation|68280|5|Briefly described|p5|Neoarchean|Neoarchean||2718-2713 Ma|Fortescue Group||overlain by Jeerinah Formation, overlies Tumbiana Formation|Basalt.|
35002|Maddina Formation|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Fortescue Group|da||Shale and siltstone, basalt basaltic andesite, andesite, komatiitic basalt, dacite and rhyolite. Basaltic to andesitic volcaniclastic sandstone, siltstone and shale.Felsic volcaniclastic sandstone and tuffaceous rocks.|
35002|Maddina Formation|69185|4|Described|GEOL_LUT_CSV files||Neoarchean|Geological Province: Pilbara Craton. Of Northwest, Northeast, and South Pilbara Sub-basins, Hamersley Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 2717 Ma|Unit of Fortescue Group.|||Massive, amygdaloidal, or vesicular basalt and basaltic andesite; local komatiitic basalt, dacite and rhyolite|
35002|Maddina Formation|69299|3|Fully described|p1,4-7,9-11,14,17,19-20,22,map|Archean|Archean|Formerly Maddina Basalt (Hickman 1983). Basaltic to rhyolitic volcanism. Thickness on COOYA POOYA: 700-1100 m. Most exposures on top of Chichester Range lie directly beneath Hamersley Surface with resultant widespread silicification, laterisation, and leaching. Geol. Prov: Hamersley Basin, Pilbara Craton.|2717 +/-2 Ma (U-Pb zircon in dacite; Nelson 1998)|Of Fortescue Group.|Includes Kuruna Member.|Conformably overlies Tumbiana Formation; is overlain by Hamersley Surface; is overlain by Jeerinah Formation 75 km west of COOYA POOYA.|Flows: massive, non-vesicular, subordinate vesicular and amygdaloidal basalt and basaltic andesite, with minor andesite, dacite and rhyolite.|14-OCT-15
35002|Maddina Formation|69301|4|Described|p16-17, p18 Fig.7, p19|||Pilbara Craton. Fortescue Basin. Northeast Pilbara Sub-basin, Northwest Pilbara Sub-basin, Sequence 3.Thickness: several hundres of metres.|ca. 2.71 Ga|Fortescue Group||Overlies Tumbiana Formation.|Dominantly volcanic. Composed of ultramafic-mafic-felsic volcanic cycles.|
35002|Maddina Formation|69411|4|Described|p282,287,290|Neoarchean|Neoarchean|Geological province: Pilbara Craton. U-Pb zircon dates of2717+\-2 Ma (Nelson, 1998; Kojan and Hickman, 1999).||Unit of Fortescue Group.||Underlain conformably by Meentheena Member/Tumbiana Formation.|Massive basalt (2-10 m); lapilli-dominated tuff, basalt flows and coarse, well-rounded clastic grains within a fine grained matrix (heavily Fe-altered).|
35002|Maddina Formation|69569|6|Mentioned|p285 Fig.1|||East Pilbara Terrane.||Fortescue Group.||||
35002|Maddina Formation|69590|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Of Northeast and Northwest Pilbara sub-basins, Fortescue Basin. Events: Pilbara Craton breakup. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_geologyp08_lut.csv.|2718-2713 Ma inferred)|Unit of Fortescue Group.|Includes Kuruna Member.||Basalt; massive, amygdaloidal, vesicular, fine-grained to doleritic; thick flows and/or sills, to thin flows; komatiitic; basaltic andesite; basaltic to andesitic volcaniclastic sandstone, siltstone and shale.|
35002|Maddina Formation|69792|5|Briefly described|p1095-6, p1097 Fig.2, p1107|||||Unit in Fortescue Group.|||Includes micritic limestone members subaerial lavas, volcaniclstic/siliciclastic rocks.|22-JUN-20
35002|Maddina Formation|70795|6|Mentioned|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean||2735-2629 Ma|||||
35002|Maddina Formation|71042|5|Briefly described|p66, p71-p72, p74|Archean|Archean|Oakover Basin, Southern Pilbara. Stretching lineation L3 is well developed in this unit. See also p76-p77, p79, p83, p86, p89-p90, p94-p95.||Fortescue Group||Overlain by Jeerinah Formation, Googhenama Formation.||28-MAY-19
35002|Maddina Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||basalt, basaltic andesite, andesite, dacite|
35002|Maddina Formation|71803|4|Described|p365-p369, p371, p374-p380, p385|Neoarchean|Neoarchean|Pilbara Craton. Geochemsitry discussed. An additional age of 2715 +/- 2 is also derived from Blake et al, 2004.  |2718 +/- 3n Ma (Blake et al, 2004)|||Laterally equivalent to the Bunjinah Formation.|Mafic lavas including subaerial (dominant) and subaqueous sheet flows with dacitic and rhyolitic volcaniclastic rocks.|
35002|Maddina Formation|71808|5|Briefly described|p8|||Pilbara Craton. Formerly the Nymerina Basalt and Maddina Basalt.||Fortescue Group|Includes the Kuruna Member.|Equivalent to the Bunjinah Formation.|Basalts and tuffaceous rocks.|
35002|Maddina Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Northeast Pilbara Sub-basin; Northwest Pilbara Sub-basin, Fortescue Basin.|Max age 2718+/-3 Ma, min 2713+/-3 Ma.|Fortescue Group, sequence 4|||Massive, amygdaloidal, or vesicular basalt and basaltic andesite; local komatiitic basalt, dacite, and rhyolite.|
35002|Maddina Formation|72489|6|Mentioned|p12|Archean|Archean|||||||
35002|Maddina Formation|72712|6|Mentioned|p8, p10 Fig.6.|Neoarchean|Neoarchean||min age c. 2715 Ma.|||Overlies Tumbiana Formation and underlies Jeerinah Formation and is equivalent to Bunjinah Formation.|Submarine basalt.|
35002|Maddina Formation|73538|6|Mentioned|p4|Neoarchean|Neoarchean|Written as Maddina Formation / Bunjinah Formation. Ages of 2715 +/- 2 Ma and 2718 +/- 3 Ma were reported by Mole et al. (2018) for these units.|2715 +/- 2 Ma, 2718 +/- 3 Ma|Fortescue Group||Underlain by Pyradie Formation / Tumbiana Formation. Overlain by Jeerinah formation.|Mafic volcanics.|
26004|Maddox Formation|22754|5|Briefly described|p11 Tb. 3|Mesoproterozoic|Mesoproterozoic|Of the Glidden Group.||||||
26004|Maddox Formation|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26004|Maddox Formation|32660|5|Briefly described|Table 6|||||||||
26004|Maddox Formation|32728|5|Briefly described|Table 6|||||||||
26004|Maddox Formation|36551|6|Mentioned|Table 10|||||||||
26004|Maddox Formation|36885|4|Described|p180|||||||||
26004|Maddox Formation|44155|5|Briefly described|p251 Tb.3-11|||90m thick.||Glidden Group|||Black shale, micaceous siltstone; minor sandstone.|
26004|Maddox Formation|44231|5|Briefly described|Map Legend|Neoproterozoic||Of the Glidden Group. Balck shale, black micaceous siltstone, purple-grey feldspathic sandstone, and purple siltstone. Geological Province: Glidden Basin.||||||30-NOV-06
26004|Maddox Formation|44397|14|Not recorded|p.15,20, Table 3||Adelaidean|Glidden Group. Defn. on Tech.File E/52-9.||||||
26004|Maddox Formation|44398|14|Not recorded|map legend||Adelaidean|||||||
26004|Maddox Formation|45047|4|Described|p35|||Glidden Group.||||||
26004|Maddox Formation|48927|2|Defined|p9|Adelaidean|Adelaidean|||||||
26004|Maddox Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Glidden Group.|||Black shale, black laminated micaceous siltstone, purple and grey flaggy fine slightly micaceous feldspathic sandstone, and purple siltstone|
78981|Madoonga Formation|69583|5|Briefly described|p49|Mesoarchean|Mesoarchean|Murchison Domain.||Weld Range Group.||||
78981|Madoonga Formation|69584|5|Briefly described|p5 Fig.2|Mesoarchean|Mesoarchean|||Weld Range Group||Overlies the Kalli Formation, overlain by the Gossan Valley Formation.|Felsic andesitic and volcanic rocks interbedded with banded iron formations.|
78981|Madoonga Formation|69586|5|Briefly described|p22|Mesoarchean|Mesoarchean|Murchison Domain.||Weld Range Group.||||
78981|Madoonga Formation|70796|5|Briefly described|100k_geologyp_lut.csv|Mesoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. An additional date provided is 2972 +/ 8 Ma (isotopic). See also 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 155879.1.pdf,|2969 +/ 4 Ma to 2979 (isoptopic)||||Psammite and pelite, interlayered; includes moderately wellbedded metasandstone; includes deeply weathered rocks. Polymictic breccia with a fine felsic volcanic matrix intruded by dolerite;  rhyolitic volcanic and volcaniclastic rocks.|
78981|Madoonga Formation|70830|5|Briefly described|p7, p9|Mesoarchean|Mesoarchean|Ages are derived from Yeats et al, 1996 and Wang et al, 1998.|c. 2975 Ma|Murchison Supergroup|||Volcano-sedimentary rocks.|
78981|Madoonga Formation|71269|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.|2972+\-8, 2969+\-4 Ma (isotopic)|Unit of Murchison Supergroup.||Coeval with Thunderlarra Supersuite/Bunnawarra Suite.|Interlayered psammite and pelite, moderately well-bedded metasandstone locally with quartz pebbles; polymictic breccia with fine felsic volcanic matrix intruded by dolerite; metamorphosed; rhyolitic volcanic and volcaniclastics, porphyric rhyolite.|
26006|Maggie Hays Formation|22583|5|Briefly described|381|Archean|Archean|Geol province Yilgarn Craton. Max thickness 2400m. Overlying unit Honman Formation||||||07-NOV-08
26006|Maggie Hays Formation|23129|5|Briefly described|p358|||Underlies Honman Formation.||||||
26006|Maggie Hays Formation|30969|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
26006|Maggie Hays Formation|31093|2|Defined|p6|Paleoarchean|Paleoarchean|||||||07-NOV-08
26006|Maggie Hays Formation|35726|6|Mentioned|p97|||||||||
26006|Maggie Hays Formation|42793|6|Mentioned|Fig.11 P241|||||||||
26006|Maggie Hays Formation|43498|5|Briefly described|2|||||||||
26006|Maggie Hays Formation|65487|5|Briefly described|p5|||Part of the Lake Johnston Greenstone Belt, locally folded into the Burmister Syncline and the Gordon Anticline. Consists of pillowed metabasalts, metamorphosed mafic/ultramafic intrusives, and minor metasediments: BIFs and volcanogenic rocks.||||||
26006|Maggie Hays Formation|68520|5|Briefly described|Map legend|Archean|Archean|Southern Cross Domain, Youanmi Terrane, Yilgarn Craton. The 7 facies variants are mapped separately.|||||Amphibolite: locally schistose, with plagioclase phenocrysts, or after basalt; metamorphosed basalt: foliated, massive, pillowed and variolitic, or flow-banded interbedded with siliciclastic and volcaniclastic sedimentary rocks.|
26006|Maggie Hays Formation|69404|5|Briefly described|p8 Fig.9, p8|||Lake Johnston greenstone belt, Southern Cross Domain. Older than 2873 Ma on the basis of stratigraphic relationship. Greater than 2km thick.||||Overlain by the Honman Formation. Intruded by the Lake Medcalf Igneous Complex.|Pillowed basalt with minor ultramafic intrusions, hyaloclastites and discontinuous quartz-rich metasedimentary rocks.|
26006|Maggie Hays Formation|69559|4|Described|100k_interpgeop_lut.csv|Mesoarchean|Mesoarchean|Southern Cross Domain, Youanmi Terrane, Yilgarn Craton. See also 100k_interpgeol_lut.csv, geologyp_lut.csv,  500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv,  geologyl_lut.csv.|3100-2873 Ma||||Fine to medium grained amphibolite; locally schistose with plagioclase phenocrysts. Foliated metabasalt, fine to medium grained. Pillowed and variolitic basalt; metamorphosed.|
26006|Maggie Hays Formation|69617|5|Briefly described|p145-149, p154-155|||Lake Johnston greenstone belt, Youanmi Terrane, Yilgarn Craton. Estimated thickness ~1600m. A variably overprinted submarine volcanic succession. Age unknown.||||Is intruded by Roundtop Komatiite and Lake Medcalf Igneous Complex.|Amphibolites (after tholeiitic basalt) with preserved pillows containing amygdales; pelites with minor metavolcaniclastic horizons; metabasalts intercalated with thin iron- and silica-rich sedimentary rocks.|
26006|Maggie Hays Formation|70144|5|Briefly described|Map legend|Archean|Archean|Southern Cross Domain, Youanmi Terrane, Yilgarn Craton. The three facies are mapped separately.|||||Fine- to medium-grained amphibolite, locally schistose; amphibolite after basalt; pillowed and variolitic basalt, metamorphosed.|
26006|Maggie Hays Formation|70153|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Mesoarchean||3100 - 2922 Ma (inferred).||||Basalt and siliciclastic sedimentary rocks; metamorphosed.|
26006|Maggie Hays Formation|70156|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3200-2600 Ma). See 500k_interpgeop14_lut.csv, 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeol_lut.csv.|3100-2920 Ma (inferred)||||Basalt and siliciclastic sedimentary rocks; metamorphosed|
26006|Maggie Hays Formation|70205|5|Briefly described|Map legend.|Archean|Archean|Southern Cross Domain, Youanmi Terrane, Yilgarn Craton. The 7 facies are mapped separately.|||||Amphibolite after basalt; foliated metabasalt; massive metabasalt; flow-banded metabasalt, locally interbedded with metasedimentary rocks; pillowed and variolitic metabasalt interbedded with metasedimentary rocks; basaltic polymictic metabreccia.|
26006|Maggie Hays Formation|70277|6|Mentioned|p799-800|Archean|Archean|Geological province: Yilgarn Craton. Part of the ~2.9 Ga Lake Johnston greenstone belt.|||||Pillowed basalt with minor ultramafic intrusions and discontinuous metasedimentary rocks.|
26006|Maggie Hays Formation|70794|4|Described|500k_interpgeop14_lut.csv,|Mesoarchean|Mesoarchean|Youanmi Terrane, Yilgarn Craton. Also 2_5m_interpgeop15_lut.csv,  500k_interpgeop_lut.csv, 100k_geologyp_lut.csv.|3131-2922 Ma inferred||||Basalt and siliciclastic sedimentary rocks; metamorphosed.Fine to medium grained amphibolite, foliated metabasalt, flow banded basalt interbedded with siliciclastic and volcaniclastic sedimentary rocks. Pillowed and variolitic basalt.|
26006|Maggie Hays Formation|70802|5|Briefly described|500k_interpgeop14_lut.csv|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Youanmi Terrane events.|3100-2922 Ma (inferred)||||Basalt and siliciclastic sedimentary rocks; metamorphosed|
26006|Maggie Hays Formation|71270|4|Described|500k_interpgeop16_lut.csv|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma); Youanmi Terrane events (3131 - 2600 Ma).|2121-2920 Ma (inferred)||||Basalt and siliciclastic sedimentary rocks; metamorphosed|
26006|Maggie Hays Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Youanmi Terrane.|||||Basalt and siliciclastic sedimentary rocks; metamorphosed.|
30828|Magotty Springs Monzogranite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  Age: c. 1835-1805 Ma.||||||07-NOV-08
30828|Magotty Springs Monzogranite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  In the Bow River batholith.  Age: 1835-1805Ma.||||||07-NOV-08
30828|Magotty Springs Monzogranite|43853|5|Briefly described|Map Legend||Proterozoic|||||||
30828|Magotty Springs Monzogranite|43855|5|Briefly described|Map Legend||Proterozoic|||||||
30828|Magotty Springs Monzogranite|44230|5|Briefly described|Map Legend||Proterozoic|||||||
30828|Magotty Springs Monzogranite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Kevins Dam Suite|||Medium- to coarse-grained, porphyritic biotite monzogranite; medium-grained, equigranular hornblende-biotite granodiorite.|31-JUL-15
30828|Magotty Springs Monzogranite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Kevins Dam Suite|||Medium-coarse grained, porphyritic biotite monzogranite; medium grained, equigranular hornblende-biotite granodiorite.|
30828|Magotty Springs Monzogranite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2.|1827-1808 Ma (Inferred)|Unit of Kevins Dam Suite.|||Medium- to coarse-grained, porphyritic biotite monzogranite; medium-grained, equigranular hornblende-biotite granodiorite|
30828|Magotty Springs Monzogranite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1808-1827 Ma|Kevins Dam Suite|||Medium- to coarse-grained, porphyritic biotite monzogranite; medium-grained, equigranular hornblende--biotite granodiorite|
30828|Magotty Springs Monzogranite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1827-1808 Ma (inferred)|Unit of Kevins Dam Suite.|||Medium- to coarse-grained, porphyritic biotite monzogranite; medium-grained, equigranular hornblende-biotite granodiorite|
30828|Magotty Springs Monzogranite|72437|5|Briefly described|p107|||Whole rock analyses are provided.||Kevins Dam Suite|||Porphyritic monzogranite.|
23749|Mahony Group|14019|6|Mentioned|p21|||Conglomerate.  Geological Province: Ord Basin.||||||
23749|Mahony Group|22537|6|Mentioned|34|Devonian|Devonian|||||||
23749|Mahony Group|22814|5|Briefly described|fig2|Late Devonian|Late Devonian|||||||
23749|Mahony Group|23621|5|Briefly described|p36|Devonian|Devonian|See also page 9 table 1. Underlying unit Headleys Limestone. Geological Province: Ord Basin.||||||
23749|Mahony Group|23622|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Ord Basin.||||||
23749|Mahony Group|23858|5|Briefly described|p919|Late Devonian|Late Devonian|Geological Province: Ord Basin. Max. thickness: >1000 m.||||||
23749|Mahony Group|24503|5|Briefly described|Map legend|Devonian|Devonian|Quartz sandstone, pebbly sandstone and pebble to boulder conglomerate.  Geological Province: Ord Basin.||||||
23749|Mahony Group|40993|6|Mentioned|Fig.1|||||||||
23749|Mahony Group|41840|3|Fully described|p44|||||||||
23749|Mahony Group|41864|4|Described|p55|||||||||
23749|Mahony Group|41865|6|Mentioned|Map legend||Frasnian|||||||
23749|Mahony Group|41866|6|Mentioned|Map legend|Frasnian||||||||
23749|Mahony Group|42030|4|Described|p750|||||||||
23749|Mahony Group|43299|5|Briefly described|Map Legend||Devonian|||||||
23749|Mahony Group|43301|5|Briefly described|Map Legend||Paleozoic|age Devonian?||||||07-NOV-08
23749|Mahony Group|43855|5|Briefly described|Map Legend||Frasnian|||||||
23749|Mahony Group|44868|5|Briefly described|Map Legend||Frasnian|||||||
23749|Mahony Group|60419|5|Briefly described|p1|Late Devonian|Late Devonian|Sandstone and minor conglomerate. Geological Province: Ord Basin.||||||
23749|Mahony Group|60519|5|Briefly described|Map Legend|Frasnian|Frasnian|Geological Province: Ord Basin. Includes: Glass Hill Sandstone.||||||
23749|Mahony Group|64580|4|Described|map legend||Frasnian|Sandstone (in places pebbly), pebble to boulder conglomerate; includes PURRALILI and GLASS HILL SANDSTONES, and BOLL CONGLOMERATE.||||||09-DEC-08
23749|Mahony Group|67860|4|Described|p416,417 Figs.4-84,85; p418 Tb. 4-18|Frasnian|Frasnian|See also p421-422. 200-1000 m thick.|||Includes Glass Hill and Purralili Sandstones, and Boll Conglomerate.|Overlies Goose Hole Group unconformably. Correlated with Cockatoo Group (Bonaparte Basin).|Quartz sandstone and conglomerate.|
23749|Mahony Group|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Frasnian|Frasnian|Ord Basin. See also 500k_geologyp08_lut.|||Includes Purralili, Glass Hill Sandstones and Boll Conglomerate.||Undivided; sandstone (pebbly in places), pebble to boulder conglomerate|
23749|Mahony Group|69099|4|Described|GEOL_LUT_CSV files + geochron files|Frasnian|Frasnian|Ord Basin|||Includes Glass Hill Sandstone, Boll Conglomerate||Sandstone (pebbly in places), and pebble to boulder conglomerate.|03-AUG-15
23749|Mahony Group|69165|4|Described|100k_interpgeop_lut.csv|Frasnian|Frasnian|See also 500k_geologyp08_lut.csv. |||Includes Glass Hill Sandstone, Boll Conglomerate, Purralili Sandstone||Undivided sandstone (in places pebbly), pebble to boulder conglomerate.|
23749|Mahony Group|69448|5|Briefly described|p33:1-3, 6-8|Late Devonian|Late Devonian|Forms the top of the Ord Basin succession in WA. Up to 1000m thick. Alluvial fan, fluviatile, aeolian, minor intertidal deposits. Probable Frasnian age. Displaced by  the NW-trending Negri Fault.||||Unconformably overlies Elder Subgroup (Goose Hole Group).|Quartz sandstone, pebbly sandstone, conglomerate; minor siltstone.|12-JUL-16
23749|Mahony Group|69587|4|Described|GEOL_LUT_CSV files|Frasnian|Frasnian|Geological province: Halls Creek Orogen, North Australian Craton. Of Ord Basin; Hardman Fold belt Events: Alice Springs Orogeny. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|||||Sandstone (pebbly in places), and pebble to boulder conglomerate|
23749|Mahony Group|69634|4|Described|GEOL_LUT_CSV files|Frasnian|Frasnian|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|382.7-372.2 Ma (Inferred)||Includes Boll Conglomerate, Glass Hill Sandstone, Purralili Sandstone.||Sandstone (pebbly in places), and pebble to boulder conglomerate|
23749|Mahony Group|70141|5|Briefly described|Map legend.|Frasnian|Frasnian|Ord Basin.|||||Sandstone, pebbly in places, and pebble to boulder conglomerate.|
23749|Mahony Group|70154|5|Briefly described|100k_interpgeop_lut.csv|Frasnian|Frasnian|See also 500k_interpgeop_lut.csv.|372-383 Ma||Includes Boll Conglomerate, Glass Hill Sandstone||Sandstone and pebble to boulder conglomerate.|
23749|Mahony Group|70826|6|Mentioned|p7 tbl 3|Devonian|Devonian|Ord Basin.||||||
23749|Mahony Group|70851|6|Mentioned|p18|||||||||
23749|Mahony Group|71146|5|Briefly described|p6|Frasnian|Givetian|Ord Basin.|||Includes the Boll Conglomerate.|Unconformably overlies the Elder Subgroup.|Sandstone.|
23749|Mahony Group|71267|4|Described|GEOL_LUT_CSV files|Frasnian|Frasnian|Geological Province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny (450-295 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma). See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|382.7-372.2 Ma (inferred)||Includes Boll Conglomerate, Galss Hill Sandstone, Purralili Sandstone.||Sandstone (pebbly in places), and pebble to boulder conglomerate|
23749|Mahony Group|71800|5|Briefly described|p25, |Devonian|Devonian|Ord Basin.||||Unconformably overlies the Overland Sandstone.||
23749|Mahony Group|72034|5|Briefly described|500k_interpgeop16_lut|Frasnian|Frasnian|Ord Basin. |||||Sandstone (pebbly in places), and pebble to boulder conglomerate.|
23749|Mahony Group|73255|6|Mentioned|p533 Fig.1, p534 Fig.2|Devonian|Devonian||||Buchanan Sandstone, Glass Hill Sandstone, Boll Conglomerate.|Disconformably overlies the Goose Hole Group, Overland Sandstone.||
75074|Mairmull Formation|67370|2|Defined|p313 Fig.2, p314, pp316-318, pp332-333.|Early Triassic|Early Triassic|New name (this study). Named after Mairmull Creek southeast of Wadeye, NT. Type section is in Fishburn-1 between 2,121 - 2,320 m. Deposited in shallow water conditions: contains Lingula, conchastracans and spinose acritarchs. Occurs throughout Bonaparte Basin and in eastern Browse Basin.||Unit in Mount Goodwin Subgroup.||Unconformably overlies Penguin Formation or Hyland Bay Sub-group. Is overlain unconformably by Ascalon Formation.|Predominantly greenish, sometimes reddish, claystone and siltstone; rare coarser sediments: thin sandstone beds in the uppermost interval.|
75074|Mairmull Formation|69452|3|Fully described|p36:8, 15, 20-21|Olenekian|Induan|Gorter et al. (2009). Equivalent to the Lower Mount Goodwin Formation of Gorter (1998) and Gorter et al. (1998). Petrel Sub-basin, Bonaparte Basin. 199m thick in the type section in drillhole Fishburn-1. Undifferentiated Ascalon Fm/Mairmull Fm forms 20m of shale and siltstone onshore, near Mount Goodwin. Has distinctive low-angle cross-lamination; contains lingulid brachiopods, estheriid conchostracens, indeterminate plants and vertebrate remains.||Mount Goodwin Subgroup.||Overlies Penguin Formation conformably or Hyland Bay Subgroup unconformably. Is overlain unconformably by Ascalon Formation.|Claystone and siltstone with rare thin sandstone interbeds, which are more common towards the top.|12-JUL-16
75074|Mairmull Formation|69454|5|Briefly described|p38:4|Olenekian|Changhsingian|Petrel Sub-basin, Bonaparte Basin.||Mount Goodwin Subgroup.||||12-JUL-16
75074|Mairmull Formation|69653|6|Mentioned|p10|Early Triassic|Early Triassic|Petrel Sub-basin.||Mount Goodwin Sub-group.||Overlies Penguin Formation. Is overlain by Ascalon Formation.||
75074|Mairmull Formation|69673|6|Mentioned|p153 fig 125|||||Mount Goodwin Subgroup||Overlain by Ascalon Formation, overlies Penguin Formation||
75074|Mairmull Formation|70061|5|Briefly described|Petrel Sub-basin Figs.2 & 3|Induan|Induan|See also Regional geology: Figs.6-8. Vulcan: Fig.2.||Mount Goodwin Subgroup.||Overlies Penguin Formation. Is overlain by Ascalon Formation.||12-JUL-16
75074|Mairmull Formation|73304|6|Mentioned|p77|||Bonaparte Basin.||||||
39911|Maitland Intrusion|24353|5|Briefly described|p7, 17|Archean|Archean|Intrudes the Whundo Group. Age: >2930Ma. Geological Province: Pilbara Craton||||||07-NOV-08
39911|Maitland Intrusion|63441|5|Briefly described|p12 Tb. 2|Archean|Archean|Of the Radley Suite. Mafic rocks.||||||07-FEB-11
39911|Maitland Intrusion|64174|5|Briefly described|Map legend|Archean|Archean|Part of the Radley Suite (Sisters Supersuite). Gabbro, leucogabbro, serpentinised peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed.||||||04-DEC-08
39911|Maitland Intrusion|64580|4|Described|map legend||Mesoarchean|Of Radley Suite. Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed.||||||15-DEC-08
39911|Maitland Intrusion|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Radley Suite.|||Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed|
39911|Maitland Intrusion|69299|6|Mentioned|p12|||c. 2925 Ma mafic-ultramafic Maitland and Radio Hill intrusions.|c. 2925 Ma||||Ultramafic.|
39911|Maitland Intrusion|70775|6|Mentioned|p66|||||||||
39911|Maitland Intrusion|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Radley Suite|||Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed.|
68668|Maitland River Supersuite|61253|5|Briefly described|p56, p52 Fig. 2|Archean|Archean|Age: >3.0Ga. Geological Province: Pilbara Craton.  See also p54-55 Fig. 3.||||||07-NOV-08
68668|Maitland River Supersuite|63441|3|Fully described|p37, p10 Tb. 2|Archean|Archean|Includes Brill, Erramurra, Hearson Cove and Waloo Waloo Monzogranites, Caines Well and Miaree Granites, Jean Well, Mardeburra and Whyjabby Granodiorites. Age: 3000-2980Ma. Geological province: West Pilbara Superterrane/Pilbara Craton. See also p33 Fig. 12||||||07-FEB-11
68668|Maitland River Supersuite|63538|6|Mentioned|p6 Fig. 3|Archean|Archean|Geological Province: Pilbara Craton.||||||19-APR-13
68668|Maitland River Supersuite|64174|5|Briefly described|Map legend|Archean|Archean|Includes 10 named granites. Age ranges included: c.2994Ma, 2995-2985Ma and 2990-2988Ma. Geological province: Pilbara Craton.||||||07-NOV-08
68668|Maitland River Supersuite|64580|4|Described|map legend||Mesoarchean|Monzogranite, minor granodiorite, locally K-feldspar porphyritic, and local gneissic granitic rocks.||||||15-DEC-08
68668|Maitland River Supersuite|64728|6|Mentioned|p97.|||||Unit in Pilbara granite-greenstone terrane.||||
68668|Maitland River Supersuite|66217|5|Briefly described|p9.|Mesoarchean|Mesoarchean|West Pilbara Superterrane. Magmatism derived from crustal melting.||||||10-JUN-20
68668|Maitland River Supersuite|67201|4|Described|p7 Fig.4, p13 Fig.8, see comments|Archean|Archean|Pilbara Craton, West Pilbara Superterrane. In De Grey Superbasin. Intrudes southern contact of Cliff Pool Tonalite (Elizabeth Hill Supersuite). Page location continued: p16-17, p19, p21-24, p44.|3000-2980 Ma|Cherratta Granitic Complex|Hearson Cove Monzogranite, Jean Well Granodiorite, Miaree Granite, Toorare Tonalite, Whyjabby Granodiorite|Intrudes southern contact of Cliff Pool Tonalite (Elizabeth Hill Supersuite). Is overlain by northwest margin units of Mallina Basin.|Includes tonalite, granodiorite and monzogranite.|
68668|Maitland River Supersuite|68035|5|Briefly described|p290-291, p290 Fig 5|Mesoarchean|Mesoarchean||3000 - 2980 Ma|||||
68668|Maitland River Supersuite|69185|5|Briefly described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.|||Includes MONZOGRANITE: Brill, Eramurra, Hearson Cove, Waloo Waloo; GRANODIORITE: Jean Well, Whyjabby; GRANITE: Caines Well, Miaree; Toorare Tonalite.|||
68668|Maitland River Supersuite|69301|5|Briefly described|p5 Fig.3, p15|||Pilbara Craton. West Pilbara Superterrane and East Pilbara Terrane. Crops out in a linear zone northwest of Whim Creek Basin.|3.00-2.98 Ga||||Granitic rocks.|
68668|Maitland River Supersuite|69590|4|Described|500k_geologyp08_lut.csv||Mesoarchean||||||Monzogranite, minor granodiorite, locally K-feldspar porphyritic, and local gneissic granitic rocks|
68668|Maitland River Supersuite|70022|6|Mentioned|p114-115|||De Grey Superbasin, West Pilbara Superterrane.|3000-2980 Ma.|||||
68668|Maitland River Supersuite|70775|4|Described|iii, p1, p8 fig 5, p9-p10, p13|Mesoarchean|Mesoarchean|Whim Creek Basin. This supersuite is more than 200 km-long and more than 50 km-long. This supersuite is the main constituent of the Dampier Granitic Complex, probably forms much of the Harding Granitic Complex and also outcrops within the Cherratta and Caines Well Granitic Complexes. Also includes Jean Well Granodiorite, Hearson Cove Monzogranite, Brill Monzogranite, Waloo Waloo Monzogranite and the Mardeburra Granodiorite. See also p15-p17, p38 -p39, p41, p44-p46, p49-p50, p53-p54, p61, p65, p80-p81.|c. 3006-2982 Ma (Van Kranendonk et al., 2006)||Includes the Whyjabby Granodiorite, Toorare Tonalite, Erramurra Monzogranite, Miaree Granite.|Intrudes the Cliff Pool Tonalite, Whundo Group, Railway Supersuite and the Orpheus Supersuite.|Tonalite, granodiorite and monzogranite.|
68668|Maitland River Supersuite|70826|6|Mentioned|p8|Mesoarchean|Mesoarchean|East Pilbara Terrane and Karratha Terrane.||||||
68668|Maitland River Supersuite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, granodiorite|
68668|Maitland River Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|De Grey Superbasin.|Max age 3006+/-12 Ma, Min 2982+/-5 Ma.||Includes Eramurra, Brill Monzogranites, Jean Well Granodiorite, Waloo Waloo, Caines Monzogranites, Whyjabby Granodiorite, Toorare Tonalite, Miaree Granite, Hearson Cove Monzogranite.||Tonalite, granodiorite, and monzogranite; K-feldspar phenocrysts in most intrusions; variably foliated; metamorphosed.|
68668|Maitland River Supersuite|72251|6|Mentioned|p52,54|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton. Of De Grey Superbasin.|3000-2980 Ma|||||
68668|Maitland River Supersuite|72668|4|Described|p4, p12, p15-17, p22, p28, p29|||West Pilbara Superterrane. Comprises most of the Cherratta, Dampier, Harding and Caines Well Granitic Complexes. Derived from crustal melting accompanying extensional basin formation.|c. 3000 Ma-2980 Ma|||Intrudes the De Grey Supergroup.|Dominated by voluminous granodiorite and monzogranite intrusions.|13-JAN-22
79541|Malcolm Metamorphics|68186|4|Described|p7-8, p26, p30, Plate 1A|Mesoproterozoic|Mesoproterozoic|Eastern Nornalup Zone, Kepa Kurl Booya Province. Previously the Malcolm Gneiss. Includes detritus aged c.1407 Ma. Part of the supracrustal rocks of the Arid Basin, which are covered by the Ragged Basin rocks (eg Mount Rugged Formation). Maximum depositional ages by Adams (2011, 2012) of migmatitic semipelitic gneiss: implications discussed. Intruded by Recherche Supersuite at 1330 +/- 14 Ma and 1314 +/- 21 Ma (Nelson, 1995). Metamorphosed at c.1311 Ma and again at c.1180 Ma. A late-stage pegmatite was dated at 1165 +/- 5 Ma.|<1455 +/- 16 Ma and 1456 +/- 21 Ma.|||Is intruded by Recherche Supersuite.|Siliciclastic metasedimentary rocks (micaceous psammite and quartzite, lesser garnet-biotite-sillimanite pelitic rocks that are locally migmatitic); also mafic amphibolitic schist and minor calc-silicate rocks with probable volcanic precursors.|
79541|Malcolm Metamorphics|68654|5|Briefly described|p3|Mesoproterozoic|Mesoproterozoic|Arid Basin, Albany-Fraser Orogen. Previously Malcolm Gneiss.|||||Metasedimentary rocks.|
79541|Malcolm Metamorphics|69003|5|Briefly described|p40|||Arid Basin, Albany-Fraser Orogen.|||||Folded green calc-silicate rocks interlayered with black mafic amphibolite.|
79541|Malcolm Metamorphics|69252|5|Briefly described|p9, p15-18, p22|||Nornalup Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen. Formerly the Malcolm Gneiss. Deformation described. Arid Basin. Crops out along a series of narrow coastal exposures. Underwent low-P high-T metamorphism (intrusion of Recherche Supersuite) at 1330 +/- 14 Ma and 1314 +/- 21 Ma (Clark et al., 2000).|1560 +/- 40 Ma (protolith max. deposition age).||||Mainly siliciclastic metasedimentary rocks (muscovite-biotite psammites); also orthogneiss, mafic amphibolite schist, quartzofeldpsathic gneiss, and minor calc-silicate rocks of possible volcanic origin.|
79541|Malcolm Metamorphics|69386|6|Mentioned|p6|||Metasediments were affected by tectonism 1345-1260 Ma.||||||
79541|Malcolm Metamorphics|69595|6|Mentioned|p3 fig 1, p19, p20, p21 fig 8, p23, |Calymmian|Calymmian|Arid Basin, eastern Nornalup Zone. Deposited in either a Fore-arc or accretionary prism setting on an oceanic substrate. Formerly the Malcolm Gneiss. Mineralogy of the mafic schist and the calc-silicates on page 20. May have been deposited in a moderate-low energy marine environment. Maximum depositional ages. See also p24 tbl 5, p24, p33, p34 fig 20, p40, p41, p42 fig 23, p43, p44, p45, p58.|1455 +/- 16 Ma, 1456 +/- 21 Ma ||||Siliciclastic metasedimentary rocks and layers of mafic amphibolite schist with less abundant calc-silicate and mafic rocks.|
79541|Malcolm Metamorphics|70023|5|Briefly described|p167,169|||Geological province: eastern Nornalup Zone; Albany-Fraser orogen. Also of Arid Basin. Metasedimentary sequence; presursors are from Mesoproterozoic Arid Basin.||||||
79541|Malcolm Metamorphics|70090|5|Briefly described|p442-445,447,449-450,452,454,461-463|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen, West Australian Craton. Of Arid Basin. Formerly known as Malcolm Gneiss (of Myers, 1995). Maximum depositional age: c. 1455 Ma (Adams 2012). Minimum depositional age: 1313+\-16 Ma intrusive microgranite. Contains c. 1807 and 1560 Ma Paleoproterozoic age components, and c. 1450 Ma Mesoproteorozoic age components.||||||
79541|Malcolm Metamorphics|70182|6|Mentioned|p3, p5|||Arid Basin, eastern Nornalup Zone, Albany-Fraser Orogen. Affected by Stage I (1330-1260 Ma) tectonism.||||||
79541|Malcolm Metamorphics|70735|6|Mentioned|p28|||Arid Basin, Fraser Zone, Albany-Fraser Orogen.||||||
79541|Malcolm Metamorphics|70802|5|Briefly described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Nornalup Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage I (1330-1260 Ma); Albany-Fraser Orogeny Stage II (1225-1140 Ma). See 500k_interpgeop14_lut.csv, 250k_pre_mesozoic_interpgeop_lut.csv.|1560+\-40 Ma; 1313+\-6 Ma||||Interbedded psammitic and pelitic schist; amphibolitic schist; minor calc-silicate rock; may include granitic dykes and intrusions|
79541|Malcolm Metamorphics|70813|6|Mentioned|p3|||Arid basin.||||||
79541|Malcolm Metamorphics|70826|6|Mentioned|p10|Mesoproterozoic|Mesoproterozoic|Albany-Fraser Orogen?||||||
79541|Malcolm Metamorphics|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Arid Basin.|Max age 1455+/-16 Ma, min 1313+/-6 Ma.|||Intruded by Recherche Supersuite.|Interbedded psammitic and pelitic schist; basalt schist locally altered to calcareous rock; intruded by Recherche Supersuite.|
79541|Malcolm Metamorphics|72059|6|Mentioned|p57|Mesoproterozoic|Mesoproterozoic|Geological province: Fraser Zone, Albany-Fraser Orogen. Of Arid Basin.||||||
79541|Malcolm Metamorphics|72710|5|Briefly described|p4 Fig.2, p13.|Mesoproterozoic|Mesoproterozoic|Shown as part of the Arid Basin. Shown as MM on p4 Fig.2. This unit is associated with Point Malcolm, and is the southeastern-most coastal exposure of Proterozoic rocks and the only known outcrop of Madura Province crust; rocks farther east are overlain by the Eucla and Bight Basins. Also misspelt as Malcom Metamorphics p13.|1600 Ma to 1310 Ma.||||Includes metasedimentary rocks.|
79541|Malcolm Metamorphics|73084|4|Described|p: 12, 55, ~63-67, 74-77, 80-82, 85...|Calymmian|Calymmian|Madura Province. Upper amphibolite to granulite grade (peak 750�C and 4 kbar, Clark et al., 2000). Shares similarities with the Sleeper Camp Formation but is slightly younger and has different relationships to granitic rocks. Granitic veins are not part of the unit; are assigned to the Recherche Supersuite instead. Age is protolith maximum depositional age. Lie within a northeast-trending fault slice that is about 40 km long and 8 km wide. Metabasalts are more common in the south, while metasedimentary rocks are dominant in the north. Interpreted as subduction-related assemblages formed in an oceanic environment. Part of the Loongana Arc. [Partly or wholly belongs to the Arubiddy Ophiolite Complex/complex?]. Report includes lithologic/petrographic description, structural analysis, whole-rock geochemistry. Also p: 87, ~119-124, 131, 139-142.|c. 1470 Ma|||Intruded by Recherche Supersuite.|Folded, psammitic, semipelitic and pelitic schistose to gneissic rocks interlayered with fine-grained, aminated metabasalt and calc-silicate rocks.|
79541|Malcolm Metamorphics|73480|6|Mentioned|p216|||Nornalup Zone, Arid Basin.||||||
23751|Malita Formation|13194|4|Described|p386 Tb. 4-16, p396 fig 4-60|Jurassic|Late Triassic|Type Section: Petrel 1 well (2229-2471m). 120-392m thick continental to marginal marine deposits.||Troughton Group||Overlies Cape Londonderry Formation or Sahul Group (both conformably). Overlain by Plover Formation (disconformably).|Red sandstone and shale; minor limestone.|
23751|Malita Formation|13224|6|Mentioned|p485 fig 3|Pliensbachian|Norian|||||||
23751|Malita Formation|13234|6|Mentioned|p250 Fig.2,p263 Tb.4, |Early Jurassic|Late Triassic|Potential reservoir.||||Overlies Cape Londonderry Formation, offshore.|Redbed fluvial sands.|
23751|Malita Formation|13354|6|Mentioned|p376 Fig.7, p379.|Late Triassic|Late Triassic|Bonaparte Basin, Petrel Sub-basin. Overlies Challis Formation.||62||||28-OCT-14
23751|Malita Formation|22663|5|Briefly described|NT97 -1-4 Fig.3||Triassic|||||||01-MAR-10
23751|Malita Formation|23377|6|Mentioned|p212 Fig.5||Late Triassic|In the Vulcan Sub-basin.||||||31-OCT-06
23751|Malita Formation|24569|5|Briefly described|p248 Fig. 3|Sinemurian|Norian|Of the Troughton Group. Geological Province: Petrel Sub-basin.||||||17-MAR-05
23751|Malita Formation|40077|6|Mentioned|Table 1|||||||||
23751|Malita Formation|41436|6|Mentioned|p44|||||||||
23751|Malita Formation|41459|6|Mentioned|Fig.2|||||||||
23751|Malita Formation|41532|3|Fully described|p304|||||||||
23751|Malita Formation|41690|5|Briefly described|p5|||||||||
23751|Malita Formation|41731|6|Mentioned|Fig.3|||||||||
23751|Malita Formation|41733|6|Mentioned|Fig.3|||||||||
23751|Malita Formation|41759|6|Mentioned|p270|||||||||
23751|Malita Formation|42034|4|Described|Fig.4 P11|||||||||
23751|Malita Formation|42056|5|Briefly described|p98|||||||||
23751|Malita Formation|42057|6|Mentioned|Fig.3 P70|||||||||
23751|Malita Formation|42081|5|Briefly described|Fig.2 P291|||||||||
23751|Malita Formation|42151|6|Mentioned|Fig.3 P57|||||||||
23751|Malita Formation|42442|2|Defined|p24|Pliensbachian|Carnian|||||||
23751|Malita Formation|43661|6|Mentioned|Fig.3|||||||||
23751|Malita Formation|43699|6|Mentioned|Fig.6,p10|Middle Jurassic|Early Jurassic|||||||
23751|Malita Formation|43705|6|Mentioned|p20|Early Jurassic|Middle Triassic|||||||
23751|Malita Formation|43739|6|Mentioned|Fig.5,p38|Early Jurassic|Triassic|||||||
23751|Malita Formation|43826|6|Mentioned|Fig.2,p163|Early Jurassic|Late Triassic|||||||01-MAR-10
23751|Malita Formation|49637|5|Briefly described|p7|Early Jurassic|Eary Jurassic|Of the Troughton Group. Fluviodeltaic siliciclastics. Geological Province: Londonderry High/Sahul Platform. See also Figs. 3 and 6.||||||29-APR-13
23751|Malita Formation|60386|6|Mentioned|p300|Early Jurassic|Late Triassic|Bonaparte Basin. Deltaic-nearshore-shelf. ||||||
23751|Malita Formation|61548|6|Mentioned|p480 Fig.3|Late Triassic|Late Triassic|Northern Bonaparte Basin.||||||
23751|Malita Formation|62837|5|Briefly described|Stratigraphic columns|Early Jurassic|Late Triassic|Of the Troughton Group.  Age: ~222-~198Ma. Geological Province:  Petrel Sub-basin (offshore).||||||01-MAR-10
23751|Malita Formation|63929|6|Mentioned|p131 Fig.2.|Late Triassic|Late Triassic|Ashmore Platform (east) and Petrel Sub-basin. Non-marine sediments with local red beds.||||Overlies Nome Formation.||
23751|Malita Formation|66124|5|Briefly described|p171 Fig.2|Rhaetian|Rhaetian|Ashmore Platform (East); also present in Petrel Sub-basin. Non-marine. Overlies Nome Formation.||||||
23751|Malita Formation|67370|6|Mentioned|p323 Fig.14.|Late Triassic|Late Triassic|Southeastern Bonaparte Basin. Type section in Petrel-1 between 2,229 - 2471 m.||Unit in Troughton Group.||Overlies Cape Londonderry Formation. Is overlain by Plover Formation.||
23751|Malita Formation|68135|5|Briefly described|p51 fig 2a|Middle Jurassic|Early Jurassic|Bonaparte Basin.||Troughton Group.||Is overlain by Plover Formation.||14-SEP-17
23751|Malita Formation|68223|6|Mentioned|p178 Fig.3|Norian|Norian|||||||
23751|Malita Formation|69452|5|Briefly described|p36:8, 15, 21|Late Triassic|Late Triassic|Petrel Sub-basin, Bonaparte Basin. Up to 300m thick. Generally non-marine, possibly arid environment.||Troughton Group.|||Red beds.|12-JUL-16
23751|Malita Formation|69454|5|Briefly described|p38:4|Rhaetian|Norian|Petrel Sub-basin, Bonaparte Basin.||Troughton Group.||||12-JUL-16
23751|Malita Formation|69456|6|Mentioned|p40:3|||Bonaparte Basin.||Troughton Group.||||12-JUL-16
23751|Malita Formation|69653|6|Mentioned|p6, 8, 10, p13 Fig.2.4, p25-27, 30|Triassic|Triassic|Petrel Sub-basin. Schematic (gamma ray) well sections. Composite well diagram. See also p41-43, 48, 50.||Troughton Group.||Overlies Cape Londonderry Formation. Is overlain by Plover Formation.||
23751|Malita Formation|69673|5|Briefly described|p153 fig 125, p173|||||Troughton Group||Overlies Cape Londonderry Formation|Sandstone, siltstone and shale.|
23751|Malita Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Bonaparte Basin.||||Overlies Mount Goodwin Sub-group.||
23751|Malita Formation|70061|5|Briefly described|Petrel Sub-basin; Fig.2|Norian|Norian|See also Regional geology: Figs.6-7, p5. Vulcan: Fig.2.||Troughton Group.||Overlies Cape Londonderry Formation. Is overlain by Plover Formation.|Fluvial sediments.|12-JUL-16
23752|Malley Spring Member|23328|5|Briefly described|1031 Fig.2|Early Cambrian|Early Cambrian|||||||07-SEP-09
23752|Malley Spring Member|40993|6|Mentioned|Fig.1|||||||||
23752|Malley Spring Member|41840|4|Described|p40, Fig.3|||||||||
23752|Malley Spring Member|41864|4|Described|p10|||||||||
23752|Malley Spring Member|41866|5|Briefly described|Map legend|Early Cambrian||||||||
23752|Malley Spring Member|65337|6|Mentioned|p94.|||||Unit in Antrim Plateau Volcanics.||||
23752|Malley Spring Member|67860|4|Described|p420 Tb. 4-18, p421 fig 4-86|Early Cambrian|Early Cambrian|Eolian deposits, 3-5 m thick. Also appears as Malley Spring Sandstone Member on p421. Type section details given. Unfossiliferous.||Antrim Plateau Volcanics|||Sandstone and siltstone.|
23752|Malley Spring Member|69445|5|Briefly described|p30:3, 17|Early Cambrian|Early Cambrian|Mory and Beere (1985). Ord Basin. Occurs about 50m above the base of the Antrim Plateau Volcanics, over a distance of 25km.||Antrim Plateau Volcanics.|||A 3-5m thick siltstone and sandstone unit.|12-JUL-16
29271|Mallina Formation|22428|6|Mentioned|2|Archean|Archean|Geol. province Pilbara||||||07-NOV-08
29271|Mallina Formation|22715|5|Briefly described|table7 p214|Archean|Archean|Age: 3000Ma.||||||07-NOV-08
29271|Mallina Formation|23046|5|Briefly described|175|||Age ca 3010 Ma||||||
29271|Mallina Formation|23244|5|Briefly described|Fig.1,2,5 p24|||of De Grey Group, Mallina Basin. Underlying unit Cleaverville Formation (u)||||||11-JUN-14
29271|Mallina Formation|23348|4|Described|218|||||||||
29271|Mallina Formation|23388|6|Mentioned|p14 Table 1|||||||||
29271|Mallina Formation|23598|4|Described|p9|Archean|Archean|Age: c.3000 Ma. Of De Grey Group. Underlain by Constantine Sandstone. Geological Province: Pilbara Craton.||||||07-NOV-08
29271|Mallina Formation|23743|4|Described|p7|Archean|Archean|Age: c.3000 Ma. Of De Grey Group. Underlying unit Constantine Sandstone. Geological Province: Mallina Basin. Max. thickness: 10,000 m.||||||07-NOV-08
29271|Mallina Formation|23783|5|Briefly described|p3|||Of De Grey Group.||||||
29271|Mallina Formation|23784|5|Briefly described|p31|Archean|Archean|Of De Grey Group.||||||07-NOV-08
29271|Mallina Formation|23789|4|Described|p18|Archean|Archean|Geological Province: Mallina Basin.||||||07-NOV-08
29271|Mallina Formation|23793|4|Described|p25|Archean|Archean|Of De Grey Group.||||||07-NOV-08
29271|Mallina Formation|23794|5|Briefly described|Map Legend|Archean|Archean|Of De Grey Group. Geological Province Pilbara Craton.||||||07-NOV-08
29271|Mallina Formation|23808|6|Mentioned|p8|||||||||
29271|Mallina Formation|23813|5|Briefly described|p111|Archean|Archean|Age: 3000-2940Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
29271|Mallina Formation|23936|5|Briefly described|p3, Fig.4|||Geological Province: Pilbara Craton. Parent: De Grey Group.||||||
29271|Mallina Formation|24025|4|Described|p8 Tb. 1|Archean|Archean|Of De Grey Group.  Max. thickness: >5000m.  Interbedded shale, siltstone and medium- to fine-grained wacke; minor chert.  Geological Province: Pilbara Craton.||||||07-NOV-08
29271|Mallina Formation|24110|5|Briefly described|Plate 1|Archean|Archean|Parent: De Grey Group.   Geological Province: Pilbara Craton||||||07-NOV-08
29271|Mallina Formation|24140|5|Briefly described|p215|||Originally of the Whim Creek Group and then included the Rushall Slate. Shale. Geological Province: Mallina Basin||||||14-SEP-05
29271|Mallina Formation|24166|4|Described|p4|Archean|Archean|Parent: De Grey Group. Geological Province: Mallina Basin||||||07-NOV-08
29271|Mallina Formation|24184|4|Described|p715|Archean|Archean|Of the De Grey Group. Overlain by Constantine Sandstone. Geological Province: Mallina Basin. Age: 2941 +/- 9Ma.||||||07-NOV-08
29271|Mallina Formation|24185|5|Briefly described|p742 Tb.4|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
29271|Mallina Formation|24189|5|Briefly described|p802 Fig.1, p803, p808|Archean|Archean|Parent: De Grey Group. Geological Province: Mallina basin||||||07-NOV-08
29271|Mallina Formation|24190|5|Briefly described|p820 Fig.1|||Parent: De Grey Group||||||
29271|Mallina Formation|24327|5|Briefly described|Map Legend|Archean|Archean|Interbedded shale, siltstone and medium- to fine-grained wacke, minor layers of chert., metamorphosed.  Parent: De Grey Group.   Age: ~2990Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
29271|Mallina Formation|24349|5|Briefly described|Map legend|Archean|Archean|Of De Grey Group.   Age: <2990Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
29271|Mallina Formation|24410|6|Mentioned|p200 Fig. 138|Archean|Archean|Metamorphosed shale. ||||||07-NOV-08
29271|Mallina Formation|24550|5|Briefly described|p36 Tb. 3.2, p154|Archean|Archean|Sandstone, slate. Age: ca 2975Ma. Geological Province: Mallina Basin, Pilbara Craton. See also p153 Fig. 7.7 (caption), p159 Fig. 7.13.||||||07-FEB-11
29271|Mallina Formation|30766|2|Defined|Appendix|Precambrian|Precambrian|||||||
29271|Mallina Formation|31310|4|Described|p55|||||||||
29271|Mallina Formation|34829|6|Mentioned|p67|||||||||
29271|Mallina Formation|36551|6|Mentioned|p69|||||||||
29271|Mallina Formation|37373|4|Described|p80|||||||||
29271|Mallina Formation|39697|6|Mentioned|p19|||See also P98||||||
29271|Mallina Formation|41073|6|Mentioned|p202|||||||||
29271|Mallina Formation|41250|5|Briefly described|p29|||||||||
29271|Mallina Formation|41252|6|Mentioned|p50|||||||||
29271|Mallina Formation|41263|6|Mentioned|p57|||||||||
29271|Mallina Formation|41635|5|Briefly described|p21|||||||||
29271|Mallina Formation|42231|4|Described|p335|||||||||
29271|Mallina Formation|43698|6|Mentioned|p26|||||||||
29271|Mallina Formation|43769|6|Mentioned|Fig.6,p861|||||||||
29271|Mallina Formation|43821|5|Briefly described|map legend|Archean|Archean|Of De Grey Group.||||||07-NOV-08
29271|Mallina Formation|44837|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
29271|Mallina Formation|44863|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
29271|Mallina Formation|50370|5|Briefly described|Map Legend|Archean|Archean|Of De Grey Group (Pilbara Supergroup). Geological Province: Pilbara Craton. Age: <2990 Ma||||||07-NOV-08
29271|Mallina Formation|60362|5|Briefly described|p1516, p1518 Fig.2|Archean|Archean|Mallina Basin.||||Conformably overlies Constantine Sandstone.|Medium- to fine-grained siliciclastic turbidites.|
29271|Mallina Formation|61253|5|Briefly described| p52 Fig. 2|Archean|Archean|Of the Croydon Group.  Age: >2.9Ga. Geological Province: Pilbara Craton.||||||07-NOV-08
29271|Mallina Formation|61267|5|Briefly described|p71|||Lateral facies equivalent of Whim Creek Group. Intruded by Peawah Granodiorite. Age: c. 3000 Ma. Geological Province: Pilbara Craton.||||||
29271|Mallina Formation|63372|4|Described|Map Legend|Archean|Archean|Of the De Grey Group. Geological Province: Whim Creek and Mallina Basin. Interbedded shale, siltstone, and medium to fine grained wacke; minor layers of chert; metamorphosed.||||||07-NOV-08
29271|Mallina Formation|63420|5|Briefly described|Map legend|Archean|Archean|Of the Croydon Group (Pilbara Supergroup). Age: c.2941Ma. Geological Province: Pilbara Craton. Interbedded shale, siltstone, sandstone, and medium- to fine-grained wacke; metamorphosed.||||||07-NOV-08
29271|Mallina Formation|63441|4|Described|p5 Tb.1, p27|Archean|Archean|Upper unit of Croydon Group (Pilbara Supergroup). Overlies Constantine Sandstone (lower unit). Intruded by granites of Portree Suite. Geological province: Mallina Basin. Comprises interbedded, well-graded, fine- to medium- grained wacke and shale.||||||07-FEB-11
29271|Mallina Formation|63538|5|Briefly described|p6 Fig. 3|Archean|Archean|Of Croydon Group. Underlain by Constantine Sandstone. Geological Province: Pilbara Craton.||||||19-APR-13
29271|Mallina Formation|63854|6|Mentioned|p230|||||Unit in De Grey Supergroup.||||
29271|Mallina Formation|64174|5|Briefly described|Map legend|Archean|Archean|Of the Croydon Group (De Grey Supergroup).  Geological province: Mallina Basin. Interbedded shale, siltsatone, sandstone and medium- to fine-grained wacke; metamorphosed.||||||07-NOV-08
29271|Mallina Formation|64580|4|Described|map legend||Mesoarchean|Of Croydon Group. Interbedded shale, siltstone, sandstone, and medium- to fine-grained wacke; metamorphosed. Basalt; locally with pyroxene spinifex texture; metamorphosed.||||||15-DEC-08
29271|Mallina Formation|65008|6|Mentioned|p2|||||Of the De Grey Group||||
29271|Mallina Formation|65415|4|Described|p119 Fig.1, p120 Fig.2, p121.|Archean|Archean|Said to overlie Mons Cupri Volcanics by Horwitz (1990) but all contacts between this unit and Whim Creek Group are tectonic. Part of this unit may correlate with Whim Creek Group.||Unit in De Grey Group.|||A sequence of fine- to medium-grained sedimentary rocks (turbidites) of arkosic sandstone and shale including thin, upward-fining interbeds which may be carbonaceous or pyritic and some layers are tuffaceous.|20-FEB-17
29271|Mallina Formation|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Mallina Basin, in De Grey Superbasin. Unit in Croydon Group. Age shown as 2997-2941 Ma. Interbedded shale, siltstone, sandstone, and medium- to fine-grained wacke; metamorphosed.||||||
29271|Mallina Formation|66217|5|Briefly described|p42.|||Mallina Basin.|||||Fine sandstone and shale.|
29271|Mallina Formation|67201|4|Described|p7 Fig.4, p12 Tb.1, p21 Fig.12, p59-60|||In northwestern Pilbara Craton, De Grey Superbasin, West Pilbara Superterrane, Mallina Basin. Folded turbidites outcrop quite poorly and discontinuously.|c. 2940 Ma|Croydon Group||Overlies Constantine Sandstone.|Turbidites. Mudstones to medium-grained sandstones.|
29271|Mallina Formation|68035|5|Briefly described|p291|Mesoarchean|Mesoarchean|Mallina Basin. 2-4 km thick.||Of Croydon Group.|||Conglomerate, sandstone, and shale deposited in submarine fans.|
29271|Mallina Formation|68281|6|Mentioned|Map Legend|Mesoarchean|Mesoarchean|Mallina Basin, De Grey Superbasin, Pilbara Craton. Age constrained by the parent Croydon Group. Age constrained by the parent Croydon Group.||Of the Croydon Group.||||11-JUN-14
29271|Mallina Formation|68283|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Mallina and Lalla Rookh Basins.|c. 2941 Ma (Smithies et al. 1999).|Of the Croydon Group.|||Interbedded shale, siltstone, sandstone, and medium- to fine-grained wacke; metamorphosed.|
29271|Mallina Formation|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Mallina Basin. Age constrained by the De Grey Supergroup.||Of the Croydon Group.|||Siliciclastic sedimentary rocks containing layers of porphyritic dacite; metamorphosed.|30-APR-14
29271|Mallina Formation|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Croydon Group|||Interbedded shale, siltstone, sandstone, and medium- to fine-grained wacke; metamorphosed. Cordierite hornfels, chlorite rich, laminated shale and siltstone; metamorphosed.|
29271|Mallina Formation|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological Province: Pilbara Craton. Of Central Pilbara Tectonic Zone; Of Mallina Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 2990-2940 Ma|Unit of Croydon Group.|||Interbedded shale, siltstone, sandstone, and medium- to fine-grained wacke; metamorphosed; basalt; locally with pyroxene spinifex texture; metamorphosed|
29271|Mallina Formation|69300|5|Briefly described|map legend|Archean|Archean|Mallina Basin||De Grey Group|||interbedded shale, siltstone, and medium- to fine-grained wacke; minor layers of chert; metamorphosed|
29271|Mallina Formation|69301|4|Described|p5 Fig.3, p9 Tb.1|||Pilbara Craton. West Pilbara Superterrane. Mallina Basin.|2940 Ma|Croydon Group|||Sedimentary rocks.|
29271|Mallina Formation|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton. Of Mallina Basin, De Grey Superbasin. Events: North Pilbara Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|3015-2931 Ma (isotopic, inferred)|Unit of Croydon Group.|||Chlorite-rich, laminated shale and siltstone; metamorphosed; cordierite hornfels, strongly contact-metamorphosed siliciclastic rocks; interbedded shale, siltstone, sandstone, and medium- to fine-grained wacke; metamorphosed.|
29271|Mallina Formation|70022|6|Mentioned|p115-116|||West Pilbara Superterrane.|2.98-2.93 Ga.|Croydon Group.|||Sub-arkose.|
29271|Mallina Formation|70775|4|Described|p12, p18, p41|Mesoarchean|Mesoarchean|Mallina Basin. Informally subdivided into an upper and lower unit. This unit is between 2.5km and 5km thick. See also p45, p54-p58, p60, p62, p68-p71.|2948 +/- 3 (Nelson, 2002e) - 2931 Ma|Croydon Group||Overlies the Constantine Sandstone and the Mount Negri Volcanics (upper). Overlain by the Cattle Well Formation (lower).|Interbedded, well-graded, fine to medium-grained wacke and shale.|
29271|Mallina Formation|71041|6|Mentioned|p45 fig 2|||||Croydon Group||Overlies the Cleaverville Formation.|Siliciclastics.|
29271|Mallina Formation|71137|6|Mentioned|p5|Archean|Archean|Up to 1300m thick.||||||
29271|Mallina Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||greywacke, sandstone, chert, shale, siltstone|
29271|Mallina Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mallina Basin.||Croydon Group|||Interbedded shale, siltstone, sandstone, and medium- to fine-grained wacke; metamorphosed.|
29271|Mallina Formation|72251|5|Briefly described|p54|Mesoarchean|Mesoarchean|Geological province: West Pilbara Superterrane, Pilbara Craton.||Unit of Bookingarra Group.||Overlain by Sisters Supersuite. Underlain by Constantine Sandstone.||
29271|Mallina Formation|72668|6|Mentioned|p4, p22|||West Pilbara Superterrane.||Croydon Group||Overlies the Constantine Sandstone.||
38040|Mallindra Well Granodiorite|24166|5|Briefly described|p15|Archean|Archean|Of the Pippingarra Granitoid Complex.||||||07-NOV-08
38040|Mallindra Well Granodiorite|24327|5|Briefly described|Map Legend|Archean|Archean|Of the Pippingarra Granitoid Complex. Geological Province: Pilbara Craton||||||07-NOV-08
38040|Mallindra Well Granodiorite|24349|5|Briefly described|Map legend|Archean|Archean|Of the Pippingarra Granitoid Complex.  Age: c.2995Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
38040|Mallindra Well Granodiorite|63420|5|Briefly described|Map legend|Archean|Archean|Of the Sisters Supersuite. Age: c.2955Ma. Geological Province: Pilbara Craton. Hornblende-biotite granodiorite; grades to tonalite; massive to moderately foliated; locally inclusion-rich; metamorphosed.||||||07-NOV-08
38040|Mallindra Well Granodiorite|63441|5|Briefly described|p11 Tb. 2, p37|Archean|Archean|Of Indee Suite (Sisters Supersuite). Age: 2946+/-3Ma. Geological province: Pilbara Craton.  Intrudes De Grey Supergroup.||||||07-FEB-11
38040|Mallindra Well Granodiorite|68283|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.||Of the Sisters Supersuite.|||Hornblende biotite granodiorite; grades to tonalite; massive to moderately foliated; locally inclusion rich; metamorphosed.|
38040|Mallindra Well Granodiorite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Sisters Supersuite|||Hornblende--biotite granodiorite and tonalite; massive to moderately foliated; locally inclusion-rich; weakly metamorphosed.|
38040|Mallindra Well Granodiorite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; North Pilbara Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3954-3919 Ma (inferred)|Unit of Sisters Supersuite.|||Hornblende-biotite granodiorite and tonalite; massive to moderately foliated; locally inclusion-rich; weakly metamorphosed|
38040|Mallindra Well Granodiorite|70775|6|Mentioned|p65|||||Indee Suite||||
38040|Mallindra Well Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite, tonaltie|
38040|Mallindra Well Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||2946+/-3 Ma |Indee Suite|||Hornblende--biotite granodiorite and tonalite; massive to moderately foliated; locally inclusion-rich; weakly metamorphosed.|
23753|Mallowa Salt|13995|5|Briefly described|p103|||In the upper part of the Carribuddy succession. Contains Tetrahedraletes medinensis (=spores of earliest land plants).|||||A very large halite evaporite body.|
23753|Mallowa Salt|13996|6|Mentioned|p149|Early Silurian|Late Ordovician|Canning basin. Mis-spelt as Mallows Salt. Age determined by Foster and Williams (1991).||||||
23753|Mallowa Salt|14228|5|Briefly described|p6 fig3|Late Ordovician|Late Ordovician|South Canning Basin.||Carribuddy Group||Overlies Nibil Formation.||05-OCT-16
23753|Mallowa Salt|22753|5|Briefly described|Fig.3 p585|Ordovician|Ordovician|||||||
23753|Mallowa Salt|24449|5|Briefly described|p741|Llandoverian|Ashgillian|Name used interchangeably with Mallowa Formation.  Geological Province: Canning Basin.||||||
23753|Mallowa Salt|40837|2|Defined|p257 Fig. 4, p273|Siegenian|Siegenian|Of the Carribuddy Group - replacing Unit B of Carribuddy Formation. Max. thickness: 695m. See also Fig. 5 page insert (p258).||||||27-JAN-10
23753|Mallowa Salt|41215|6|Mentioned|Fig.4|||||||||
23753|Mallowa Salt|42030|6|Mentioned|p746|||||||||
23753|Mallowa Salt|42338|3|Fully described|p144|||||||||
23753|Mallowa Salt|42792|5|Briefly described|Table 1 P225|||||||||
23753|Mallowa Salt|43563|6|Mentioned|Fig.2,p5|||||||||
23753|Mallowa Salt|43599|6|Mentioned|p250, Fig.3||Ashgillian|||||||
23753|Mallowa Salt|43656|6|Mentioned|Fig.2,p8|Ashgillian|Ashgillian|||||||
23753|Mallowa Salt|43666|6|Mentioned|p9|||||||||
23753|Mallowa Salt|43746|6|Mentioned|Fig.2,p11|Ashgillian|Ashgillian|||||||
23753|Mallowa Salt|43818|6|Mentioned|Fig.2.p39||Silurian|||||||
23753|Mallowa Salt|44143|4|Described|p.440 Table 4-19, p442 Fig.4-96|Devonian|Silurian|Unit in Carribuddy Group. Up to 534m thick; halite and minor dolomite; sabkha and supratidal marine. Conformable on Nibil Formation. Type section between 2967 and 3501m in Kidson 1 (URAL: 22deg 37' 27" S, 125deg 00' 17" E). Contains sparse spores & pollen.||||||23-NOV-17
23753|Mallowa Salt|61021|5|Briefly described|p36 Fig. 2|Ashgillian|Ashgillian|Thick evaporitic section. Geological Province: Canning Basin. See also p39.||||||17-DEC-07
23753|Mallowa Salt|61551|5|Briefly described|p351 Fig.2, p359.|Ruddanian|Late Ordovician|||Unit in Carribuddy Group.||Overlies Nibil Formation. Is overlain by Sahara Formation.|Evaporites.|
23753|Mallowa Salt|64334|5|Briefly described|p39, 41|Ordovician|Ordovician|Canning Basin; subsurface only. Ashgill.||Carribuddy Group.||Overlies Nibil Formation. Is overlain by Sahara Formation.|Halite.|
23753|Mallowa Salt|64643|5|Briefly described|p3 Fig. 2|Llandovery|Upper Ordovician|Of Carribuddy Group?||||||
23753|Mallowa Salt|64982|5|Briefly described|p699 Fig.4, p701.|Llandovery|Ashgill|Up to 695 m of saltern deposits. Contains palynomorphs. Acts as seal for Nita Formation hydrocarbon reservoir.||Unit in Carribuddy Group.||Overlies Nibil Formation. Is overlain by Sahara Formation.|Cyclic, massive halite and dolomite.|
23753|Mallowa Salt|65301|5|Briefly described|p3, p5 Fig. 4, p6|Late Ordovician|Late Ordovician|Thickness: 370m. Geological province: Canning Basin, including Kidson Sub-basin and Broome Platform. Forms a super-seal over underlying Ordovician units||||||
23753|Mallowa Salt|65449|3|Fully described|p1, p5-10, p13-14, p17, p19, p21, p23-28|Llandovery|Late Ordovician|See also p38, p40, p47-50, p53-57; Plates 1-5, 7-11. Lehmann (1984), after Mallowa Native Well. Type section is the interval 3501-2967m in Kidson 1. A firm age-constraint is from Late Ordovician or earliest Silurian tetrad land plant spores (Tetrahedraletes medinensis). Potential as a seal and as source of potash. Up to 800m thick; covers c.180 000km2: is the most voluminous halite formation in Australia. High gas reading reported from Leo 1. Biostratigraphic data detailed.||Carribuddy Group.||Conformably overlies Nibil Formation. Is overlain conformably by Sahara Formation.|Beds of halite interbedded with red, green, grey and black organic-rich mudstone; with lesser anhydrite and dolomite. It is notably cyclic.|
23753|Mallowa Salt|68007|4|Described|p2, p4-5, p11, p13, p15, Plate 1|Llandovery|Ordovician|Canning Basin. Type section is in WAPET's Kidson 1 stratigraphic well. Forms a regional seal. Contains the spore Tetrahedraletes mediensis and the acritarch Rugaletes.||Carribuddy Group.||Overlies Nibil Formation. Is overlain by Sahara Formation.||24-FEB-20
23753|Mallowa Salt|68902|5|Briefly described|p9 fig 6, p26|Silurian|Ordovician |||Carribuddy Group||Overlies Nibil Formation; overlain by Sahara Formation.||
23753|Mallowa Salt|69182|6|Mentioned|Ch4 p9-p12, Ch4 p38|Upper Ordovician|Upper Ordovician|Canning Basin. This unit may act as a potential carbon dioxide seal. See also Ch4 p40-p41, Ch4 p45, Ch4 p47-p48, Ch4 p50-p58, Ch4 p74, Ch4 p79-p82, Ch4 p92, Ch4 p94. ||Carribuddy Group||Overlies the Nibil Formation. Overlain by the Sahara Formation.||
23753|Mallowa Salt|69312|6|Mentioned|p19|Llandovery|Late Ordovician|Canning Basin. Misspelt as Mallawo Salt except p19. See also  p25 fig 30, p27 fig 34, p28 fig 36.||Carribuddy Group||Overlies the Nibil Formation. Overlain by the Sahara Formation.|Salt.|11-FEB-20
23753|Mallowa Salt|69883|5|Briefly described|p4-p5|Ashgill|Ashgill|Canning Basin. Supersequences provided. Marginal marine barred-basin setting. Contains age-diagnostic fossils in the form of Late Ordovician - Early Silurian palynomorphs.||Carribuddy Group||Overlies the Nibil Formation. Overlain by the Sahara Formation.|Halite deposits.|26-FEB-20
23753|Mallowa Salt|70774|5|Briefly described|p4|Llandovery|Late Ordovician|Willara and Kidson Sub-basins, Canning Basin.||Carribuddy Group||Overlies the Nibil Formation. Overlain by the Sahara Formation.||06-FEB-20
23753|Mallowa Salt|71146|5|Briefly described|p6, p45|Late Ordovician|Late Ordovician|Canning Basin.||Carribuddy Group|||Halite, evaporite.|
23753|Mallowa Salt|71171|6|Mentioned|p2|||Canning Basin.||||||
23753|Mallowa Salt|71894|5|Briefly described|p4, p6|Silurian|Upper Ordovician|Canning Basin.||Carribuddy Group||Overlies the Nibil Formation. Overlain by the Sahara Formation.|Salt (evaporite).|
23753|Mallowa Salt|72497|5|Briefly described|p3 Fig.2.|Hirnantian|Katian|Shown as occuring in the Anketell, Tabletop, Ryan Shelves, Willara and Kidson Sub-basins, the Jurgurra and Barbwire Terraces and Broome Platform. Age shown as Ashgillian= Bolindian (Aust), Katian - Hirnantian (ICS).||Carribuddy Group||Conformably overlies Nibil Formation, conformably underlies Sahara Formation, unconformably underlies Worral Formation.||
23753|Mallowa Salt|72499|5|Briefly described|p7 Fig.6.|Llandovery|Late Ordovician|Located in the Willara Sub-basin and the Broome Platform.||Carribuddy Group||Overlies Nibil Formation and underlies Sahara Formation.|Includes evaporites.|
23753|Mallowa Salt|72504|6|Mentioned|Figure 3|||Canning Basin, Broome Platform. Intersected in the Looma 1, Fruitcake 1 drillholes.||Of Carribuddy Group.||||18-MAR-20
23753|Mallowa Salt|73117|5|Briefly described|p3, p113, p141|Llandovery|Upper Ordovician|Canning Basin.||Carribuddy Group||Underlain by Nibil Formation. Overlain by Sahara Formation.|Dominantly evaporite, salt.|
23753|Mallowa Salt|73344|6|Mentioned|p6|Hirnantian|Katian|Canning Basin, subsurface. Part of supersequence B2.||Carribuddy Group||Underlain by Nibil Formation. Overlain by Sahara Formation.||
74715|Malmac Granite|63866|5|Briefly described|p167|Statherian|Statherian|Malmac Inlier.|1724 +/-24 Ma (SHRIMP U-Pb zircon)|||||
74715|Malmac Granite|64580|4|Described|map legend|Neoarchean|Neoarchean|Weathered monzogranite.||||||17-NOV-08
74715|Malmac Granite|64655|5|Briefly described|Map Legend|Archaean|Archaean|Comprises monzogranite, weathered; foliated and cut by quartz veins near contact with country rock. Geological Province: Yilgarn Craton.||||||
74715|Malmac Granite|64772|5|Briefly described|p8, Plate 1  legend|Archean|Archean|Age: c.2550Ma (SHRIMP zircon). Geological province: Malmac Inlier, Yilgarn Craton. Weathered monzogranite cut by quartz veins near contact with country rock.||||||01-MAR-11
74715|Malmac Granite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||||||Weathered monzogranite.|
78531|Maloneys Dam Metagranite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||3010 - 2600 Ma (inferred).||||Biotite-bearing metagranite.|
78531|Maloneys Dam Metagranite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2655-2600 Ma (inferred)||||Biotite-bearing metagranite|
28717|Mamilu Hill Lamproite|41158|6|Mentioned|Table 49|||||||||
23759|Mandorah Shale|37016|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
23759|Mandorah Shale|39427|2|Defined|p4|Precambrian|Precambrian|||||||
23759|Mandorah Shale|40900|6|Mentioned|p32|||||||||
23759|Mandorah Shale|44142|5|Briefly described|p326 Tb.4-5|||500 m thick.||Uaroo Group.||Correlated with Kiangi Creek Formation.|Shale, chert.|
23759|Mandorah Shale|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||chert, shale|
25200|Mandy Calcarenite|35282|6|Mentioned|p27|||||||||
23761|Manfred Complex|22694|5|Briefly described|p6|Archean|Archean|||||||07-NOV-08
23761|Manfred Complex|23569|6|Mentioned|p3|||Structural term.||||||
23761|Manfred Complex|23781|4|Described|p11|Archean|Archean|Of the Narryer Gneiss Complex?  Age: 3730Ma (SHRIMP U-Pb).||||||07-NOV-08
23761|Manfred Complex|24114|5|Briefly described|p6|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
23761|Manfred Complex|24160|5|Briefly described|p64, p66|Archean|Archean|Inclusions of this unit occur in Dugel and Meeberrie Gneisses.|||||Mafic-ultramafic layered intrusions; abundant amphibolite (metagabbro), metamorphosed and serpentinized dunite, peridotite and pyroxenite.|
23761|Manfred Complex|40101|5|Briefly described|p158|||||||||
23761|Manfred Complex|40588|6|Mentioned|p350|||||||||
23761|Manfred Complex|40661|6|Mentioned|p95|||||||||
23761|Manfred Complex|41261|3|Fully described|p3|||||||||
23761|Manfred Complex|41331|4|Described|p299|||||||||
23761|Manfred Complex|41332|6|Mentioned|p311|||||||||
23761|Manfred Complex|41333|5|Briefly described|p334|||||||||
23761|Manfred Complex|41334|5|Briefly described|p344|||||||||
23761|Manfred Complex|41942|6|Mentioned|p52|||||||||
23761|Manfred Complex|42800|6|Mentioned|p68|||||||||
23761|Manfred Complex|43595|5|Briefly described|p224|||Age: approx. 3730 Ma||||||
23761|Manfred Complex|44149|4|Described|p15, p18-21, p24|Eoarchean|Eoarchean|Contains earth's oldest anorthosite, igneous textures, igneous-layering structures and igneous-mineral assemblages. A layered gabbro-anorthosite complex. Other ages given. Inclusions in Dugel and Meeberrie Gneisses range from individual plagioclase crystals to layers of rock to 1000m length.|3730 Ma (Zircon U-Pb; Kinny et al., 1987).|Narryer Gneiss Complex (oldest part of)||Occurs as inclusions within Dugel Gneiss and Meeberrie Gneiss.|Deformed and recrystallised: metamorphosed anorthosite, leucogabbro, gabbro and ultramafic rocks. Mostly metagabbro and amphibolite. Ultramafics are mostly serpentinised.|
23761|Manfred Complex|60694|5|Briefly described|p253|Archean|Archean|Dismembered enclaves contained within the Meeberrie and Dugel gneisses.  Age: 3730+/-6Ma (zircon).  Geological Province: Narryer Terrane/Yilgarn Craton.||||||07-NOV-08
23761|Manfred Complex|64771|5|Briefly described|p7|Eoarchean|Eoarchean|One of the oldest components of Narryer Terrane: a dismembered layered igneous complex.|3730 Ma.||Dugel gneiss.|Is intruded by Dugel and Eurada gneisses.|Anorthosite-gabbro-ultramafic intrusion.|
23761|Manfred Complex|65915|5|Briefly described|p19|Paleoarchean|Paleoarchean|In Narryer Terrane of the Yilgarn Craton. 3730 Ma: contains oldest known rocks in Australia.||||||
23761|Manfred Complex|66299|4|Described|p28.|Archean|Archean|Fragments are contained within Meeberrie Gneiss and unnamed granitic gneisses of Narryer Terrane, Yilgarn Craton.|||||Heterogeneously deformed and metamorphosed layered anorthosite, leucogabbro, gabbro, melanogabbro, ultramafic rocks.|
23761|Manfred Complex|67129|5|Briefly described|p4, p55|Archean|Archean|Myers and Williams (1985). Narryer Terrane. A dismembered layered basic intrusion, hosted by the Dugel Gneiss.|3730 +/- 6 Ma (U-Pb zircon: Kinny et al., 1988).||||Includes anorthosite.|
23761|Manfred Complex|68108|6|Mentioned|p625, p628|Eoarchean|Eoarchean|Narryer Terrane, western Yilgarn Craton.|ca. 3730 Ma|||||
23761|Manfred Complex|68123|6|Mentioned|p30, 32, 35-37, 41-42|Archean|Archean|Narryer Terrane, Yilgarn Craton.|c.3730 Ma.||||Dismembered layered mafic intrusions of meta-anorthosite and deformed leucogabbro.|
23761|Manfred Complex|69080|5|Briefly described|p688|||Narryer Terrane, Yilgarn Craton. Oldest rocks in Australia. The Narryer Terrane also contains the oldest detrital zircons on Earth: c.4400 Ma (Wilde et al., 2001).|c.3730 Ma.|||||
23761|Manfred Complex|69387|6|Mentioned|p2|||Narryer Terrane.|c.3730 Ma.|||||
23761|Manfred Complex|69583|4|Described|p54|||Myers and Williams (1985). One of the oldest components of the Narryer Terrane. The 3730 Ma age (magmatic SHRIMP U-Pb zircon) is from Manfred Complex inclusions in the Dugel Gneiss. Underwent deformation, and amphibolite to granulite facies metamorphism, at c.3300 Ma.|3730 +/- 6 Ma (Kinny et al., 1988).|||Intruded by Dugel and Eurada Gneisses (felsic magma protoliths).|A dismembered layered igneous complex (anorthosite-gabbro-ultramafic intrusion).|
23761|Manfred Complex|69596|6|Mentioned|p5|||Narryer Terrane. Oldest rocks in Australia.|c.3730 Ma.|||||
23761|Manfred Complex|70500|6|Mentioned|p126|Eoarchean|Eoarchean||3730 Ma (anorthosite; SIMS: Kinny et al., 1991).|||||
23761|Manfred Complex|70826|6|Mentioned|p4|Eoarchean|Eoarchean||ca. 3730 Ma||||Anorthosite-gabbro-ultramafic igneous rocks.|
23761|Manfred Complex|70830|6|Mentioned|p28|Eoarchean|Eoarchean|Narryer Terrane.|3730 +/- 6 Ma|||||
23761|Manfred Complex|71168|5|Briefly described|p6|Eoarchean|Eoarchean|Narryer and South West Terranes, Yilgarn Craton.|c. 3700 Ma|||Intruded by the Dugel and Eurada Gneisses.||
31474|Mangles Member|12758|5|Briefly described|p21, p10 Fg. 10|Early Cretaceous|Early Cretaceous|Of the Carnac Formation. A 915m incomplete interval of this member is present in borehole Roe 1. Unconformably overlain by South Perth Shale. Thickness in type section: 872m. Geological Province: Vlaming Sub-basin.||||||28-JUL-09
31474|Mangles Member|14227|5|Briefly described|Enclos. 2|Berriasian|Berriasian|Of Carnac Formation (Parmelia Group). Overlies Stragglers Member, underlies Hawley Member. Presented as Mangles.||||||07-FEB-11
31474|Mangles Member|24443|5|Briefly described|Fig.31|Early Cretaceous|Late Jurassic|Of Carnac Formation. Conformably overlies Stragglers Member. Conformably overlain by Hawley Member. Geological Province: Perth Basin.||||||
31474|Mangles Member|50108|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Carnac Formation (Parmelia Group). Geological Province: Perth Basin.||||||28-JUL-09
31474|Mangles Member|69182|6|Mentioned|Ch2 p15|Lower Cretaceous|Lower Cretaceous|Perth Basin. ||Carnac Formation||||
31474|Mangles Member|70128|5|Briefly described|p463 Fig.10|Early Cretaceous|Early Cretaceous|Vlaming Sub-basin.||Carnac Formation.||||
31474|Mangles Member|71958|5|Briefly described|p14, p41, p45-p46|Early Cretaceous|Early Cretaceous|Vlaming Sub-basin. A small accumulation of dry gas was discovered in this unit in the Marri 1 drillhole.||Carnac Formation||||
36848|Manyutup Tonalite|23727|4|Described|p11|Archean|Archean|See also Manyutup Tonalite Complex?||||||07-NOV-08
36848|Manyutup Tonalite|23752|4|Described|p8|Archean|Archean|Geological Province: Ravensthorpe Terrane.||||||07-NOV-08
36848|Manyutup Tonalite|23753|5|Briefly described|Map Legend|Archean|Archean|Tonalitic complex.  Geological Province: Yilgarn Craton.||||||07-NOV-08
36848|Manyutup Tonalite|23754|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
36848|Manyutup Tonalite|24165|6|Mentioned|p31, p53|||Hosts some significant gold mines. Most mineralisation is confined to marginal parts of the pluton.|||||Coarse-grained tonalite.|
36848|Manyutup Tonalite|50542|6|Mentioned|p123|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-FEB-11
36848|Manyutup Tonalite|64580|4|Described|map legend|Archean|Archean|Tonalite; minor phases of diorite and granodiorite; metamorphosed.||||||15-DEC-08
36848|Manyutup Tonalite|65487|6|Mentioned|p6|Archean|Archean|Included in the Ravensthorpe Suite, thought to be co-magmatic with the Annabelle Volcanics. Dominated by coarse-grained equigranular biotite-hornblende tonalite, varies to include dioritic and granodioritic compositions; minor phases include quartz-diorite, microtonalite, hornblendite, anorthositic gabbro. Age 2966 +/- 12 Ma (Savage et al., 1996).||||||
36848|Manyutup Tonalite|68186|5|Briefly described|p14|Archean|Archean|Yilgarn Craton.||||Is overlain non-conformably by Steere Formation.||
36848|Manyutup Tonalite|69252|5|Briefly described|p10-11|||Yilgarn Craton.||||Is overlain nonconformably (or thrust-fault) by Steere Formation.||
36848|Manyutup Tonalite|69595|6|Mentioned|p8, p11 tbl 2|Archean|Archean|Yilgarn Craton.||||Non-conformably overlain by the Steere Formation.||
36848|Manyutup Tonalite|70020|6|Mentioned|p127|Mesoarchean|Mesoarchean|Synvolcanic. Hosts Cu-Zn mineralisation. Ages from Witt 1999: 2965+\-12 Ma and 2989+\-7 Ma.||||||
36848|Manyutup Tonalite|70090|6|Mentioned|p446,448|||Geological province: Biranup Zone, Albany-Fraser Orogen, West Australian Craton. ||||Overlain by Steere Formation.||
36848|Manyutup Tonalite|70802|5|Briefly described|500k_interpgeop14_lut.csv|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Youanmi Terrane events.|2989+\-7 Ma; 1965+\-12 Ma||||Tonalite; minor phases of diorite and granodiorite; metamorphosed|
36848|Manyutup Tonalite|71168|5|Briefly described|p17, p50|||Ravensthorpe greenstone belt. Forms the Ravensthorpe 'Terrane' with the Annabelle Volcanics.|2989 +/- 7 Ma (U-Pb, Savage et al., 1995)|||||
36848|Manyutup Tonalite|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||tonalite, quartz diorite, dolerite|
36848|Manyutup Tonalite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Youanmi Terrane.|Max age 2989+/-7 Ma, min 2965+/-12 Ma.||||Tonalite; minor phases of diorite and granodiorite; metamorphosed.|
39346|Maori Queen Tonalite|24091|4|Described|p66|Archean|Archean|Age: 2703+/-5Ma (Pb/Pb). Geological Province: Yilgarn Craton.||||||07-NOV-08
39346|Maori Queen Tonalite|24196|5|Briefly described|p45|Archean|Archean|Age: 2703 +/- 5 Ma (Fletcher et al., 2001)||||||07-NOV-08
75533|Mapa Igneous Complex|66117|5|Briefly described|Map legend|Archean|Archean|Merolia Domain, Burtville Terrane, Yilgarn Craton. c.2755 Ma. Comprises several units: schist, amphibolite, schistose metapyroxenite, metadolerite, metagabbro, metamorphosed pyroxene-rich cumulate rock.||||||
75533|Mapa Igneous Complex|66195|5|Briefly described|p610, p611 Fig.9|Neoarchean|Neoarchean|Burtville Terrane.  2755 +/- 5 Ma. Mafic volcanics.||||||13-MAR-12
75533|Mapa Igneous Complex|67129|5|Briefly described|p55|Archean|Archean|Burtville Terrane, Eastern Goldfields Superterrane.|2755 +/- 5 Ma.|||||
75533|Mapa Igneous Complex|68107|4|Described|p607 Fig.3, p609 Tb.1, p610, p613 Fig.6.|Neoarchean|Neoarchean|Mount Venn Greenstone Belt, Burtville Terrane. Contains xenocrysts dated at c. 2932 Ma (Wingate et al. 2011). A layered body which is at least 400m thick (the upper contact is not preserved).|2755 +/- 5 Ma (Wingate et al. 2011).||||Contains two lower gabbroic layers that grade from  pyroxenite through melanocratic gabbro to more leucocratic gabbro at the top, and an upper layer of homogeneous, medium-grained dolerite.|22-SEP-14
75533|Mapa Igneous Complex|68109|6|Mentioned|p665|Neoarchean|Neoarchean|Burtville Terrane. Contains zircons that show evidence of juvenile input.|ca. 2755 Ma|||||
75533|Mapa Igneous Complex|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Merolia Domain, Burtville Terrane, Eastern Goldfields Superterrane, Yilgarn Craton|||Includes 6 unnamed subunits.||Schist from mafic intrusives; amphibolite, from gabbro and dolerite; schistose metapyroxenite; dolerite; minor basalt or gabbro; gabbro; common leucogabbro, minor pyroxenite; pyroxene-rich cumulate rock; locally schistose;  all metamorphosed|06-AUG-15
75533|Mapa Igneous Complex|69404|6|Mentioned|p4 Fig.4|Neoarchean|Neoarchean|Burtville Terrane.|c. 2750 Ma|||||
75533|Mapa Igneous Complex|69617|6|Mentioned|p154|||Burtville Terrane, Eastern Goldfields Superterrane.||||||
75533|Mapa Igneous Complex|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|See also 100k_geologyp14_lut.csv and 500k_interpgeop14_lut.csv. Age derived from metagabbro sample and is age of magmatic crystallisation of gabbro protolith (185976.1.pdf) |2755 +/- 5 Ma (SHRIMP).||||Schist derived from mafic intrusive rock, amphibolite derived from gabbro and dolerite. Schistose metapyroxenite, dolerite. Gabbro; common leucogabbro and minor pyroxenite components. Pyroxene rich cumulate rock; locally schistose; metamorphosed.|
75533|Mapa Igneous Complex|70826|6|Mentioned|p8|Neoarchean|Neoarchean|eastern Yilgarn Craton.||||||
75533|Mapa Igneous Complex|71168|6|Mentioned|p10|Neoarchean|Neoarchean|Burtville Terrane, Yilgarn Craton.|2755 +/- 5 Ma|||||
75533|Mapa Igneous Complex|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Burtville Terrane.|||||Layered gabbro and dolerite with minor pyroxenite; generally weakly metamorphosed, locally up to amphibolite facies; locally schistose.|
75533|Mapa Igneous Complex|73596|6|Mentioned|p1170|Neoarchean|Neoarchean|Mount Venn Greenstone Belt, Burtville Terrane.|2755 +/- 5 Ma.|||||
27828|Maraloou Formation|7161|6|Mentioned|p100|||||||||
27828|Maraloou Formation|7471|5|Briefly described|p8, Map legend|Proterozoic|Proterozoic|Yerrida Basin. Small outcrops WNW of Wiluna.||Of the Mooloogool Subgroup.||Overlies Killara Formation.|Black shales, siltstones, and carbonate rocks.|
27828|Maraloou Formation|12099|5|Briefly described|p677-8, 680-1, 683, 686, Figs.2, 4, 5,6|Paleoproterozoic|Paleoproterozoic|Yerrida Basin. Placed in Glengarry Group by Gee (1987) and Gee and Grey (1993).||Of Mooloogool Subgroup.||Overlies or locally intercalated with Killara Formation. Contact between underlying Killara Formation and Maraloou Formation is transitional to unconformable in the eastern Yerrida Basin.|Includes argillite units and black shales.|04-MAR-13
27828|Maraloou Formation|22493|6|Mentioned|p100|||||||||
27828|Maraloou Formation|22940|4|Described|Fig.1 p3|||See also Table 2 p12. of Mooloogool Subgroup, Yerrida Group.||||||
27828|Maraloou Formation|23133|4|Described|p293 Fig.1|||of Yerrida Basin.||||||25-SEP-15
27828|Maraloou Formation|23151|5|Briefly described|p67|||of Yerrida Group.||||||
27828|Maraloou Formation|23561|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Mooloogool Subgroup,Yerrida Basin||||||07-NOV-08
27828|Maraloou Formation|23581|5|Briefly described|Map legend|||Of the Mooloogool Subgroup in the Yerrida Group in the Yerrida Basin||||||
27828|Maraloou Formation|23589|4|Described|p19|||Uppermost unit of the Yerrida Group. Of Mooloogool Subgroup. Underlying unit Killara Formation. Max. thickness 100 m.||||||
27828|Maraloou Formation|23593|4|Described|p17|||Of Mooloogool Subgroup. Underlying unit Killara Formation. Geological Province: Yerrida Basin. Max. thickness: ~1000 m.||||||
27828|Maraloou Formation|23597|5|Briefly described|p2 Fig 1|||Of Yerrida Group. Geological Province: Yerrida Basin.||||||
27828|Maraloou Formation|23600|4|Described|p16|Proterozoic|Proterozoic|Of Mooloogool Subgroup. Underlying unit Killara Formation. Geological Province: Yerrida Basin. Max. thickness: 1000 m.||||||
27828|Maraloou Formation|23744|5|Briefly described|p10 Table 1|Paleoproterozoic|Paleoproterozoic|Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||07-NOV-08
27828|Maraloou Formation|23747|5|Briefly described|p4 table 1|Paleoproterozoic|Paleoproterozoic|Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||07-NOV-08
27828|Maraloou Formation|23749|5|Briefly described|p3 table 1|Proterozoic|Proterozoic|Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||
27828|Maraloou Formation|23865|5|Briefly described|p170|Paleoproterozoic|Paleoproterozoic|Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||07-NOV-08
27828|Maraloou Formation|24021|4|Described|p16|Paleoproterozoic|Paleoproterozoic|Parent: Mooloogool Subgroup. Geological Province: Yerrida Basin||||||14-APR-11
27828|Maraloou Formation|24022|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Mooloogool Subgroup, Yerrida Group. Geological Province: Yerrida Basin.||||||07-NOV-08
27828|Maraloou Formation|24028|4|Described|p289|Paleoproterozoic|Paleoproterozoic|Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||14-APR-11
27828|Maraloou Formation|24535|5|Briefly described|p22|Paleoproterozoic|Paleoproterozoic|Geological Province: Yerrida Basin. Wet sediment intruded by dolerite sill at 1843 +/- 10 Ma, which indicates this age close to time of deposition. Misspelt as Maralou Formation in Fig.18 p23.|~1843 +/- 10 Ma U/Pb SHRIMP dolerite emplacement|Of the Mooloogool Group.|||Sulphidic shale, laminated siltstone and minor sandstone and carbonate.|20-FEB-17
27828|Maraloou Formation|30010|4|Described|p45|||||||||
27828|Maraloou Formation|35975|6|Mentioned|p100|||||||||
27828|Maraloou Formation|36551|6|Mentioned|Table 29|||||||||
27828|Maraloou Formation|37460|5|Briefly described|p143|||||||||
27828|Maraloou Formation|38880|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27828|Maraloou Formation|38881|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27828|Maraloou Formation|38994|3|Fully described|p27|||||||||22-DEC-09
27828|Maraloou Formation|40937|6|Mentioned|p28|||||||||
27828|Maraloou Formation|40938|5|Briefly described|p10|||Mention Fig.5||||||
27828|Maraloou Formation|40989|6|Mentioned|p13|||||||||
27828|Maraloou Formation|43069|1|Redefined|p30|Mesoproterozoic|Paleoproterozoic|refer to Bunting et al.(1977) for original definition.||||||07-NOV-08
27828|Maraloou Formation|43238|5|Briefly described|p6|||||||||
27828|Maraloou Formation|43836|5|Briefly described|Map Legend||Proterozoic|||||||
27828|Maraloou Formation|43837|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mooloogool Subgroup (Yerrida Group).  Thin-bedded siltstone and black shale.||||||18-MAY-04
27828|Maraloou Formation|44204|5|Briefly described|Map Legend||Proterozoic|||||||
27828|Maraloou Formation|49893|4|Described|p16|Proterozoic|Proterozoic|Of the Mooloogool Subgroup (Yerrida Group). Geological  Province: Yerrida Basin. Intercalated with the Killara Formation. See also p2 Fig.1.||||||
27828|Maraloou Formation|49896|5|Briefly described|p2 Tb. 1|||Of Bunting et al (1977).||||||
27828|Maraloou Formation|49912|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Yerrida Group.  Geological Province: Yerrida Basin.||||||
27828|Maraloou Formation|50222|5|Briefly described|p320 Fig. 3, p323|Paleoproterozoic|Paleoproterozoic|Of the Mooloogool Group. Overlies the Killara Formation. Age: 1.84Ga (Rasmussen and Fletcher, 2002). Max. thickness: ~1000m. Geological Province: Yerrida Basin. See also p319 Fig. 2.||||||14-APR-11
27828|Maraloou Formation|50223|5|Briefly described|p349|Paleoproterozoic|Paleoproterozoic|Age: 1843+/-14Ma (Rasmussen and Fletcher, 2002).  Geological Province: Yerrida Basin.||||||07-NOV-08
27828|Maraloou Formation|61271|5|Briefly described|p105 Fig.1, p106|||Of the Mooloogool Subgroup. Largely shale with dolomitic intercalations locally replaced by chert.||||||
27828|Maraloou Formation|62289|4|Described|plate 1, p3-4, p7-8, p12, 19, p26-29|Palaeoproterozoic|Palaeoproterozoic|Uppermost of Mooloogool Subgroup (Yerrida Group); gradationally overlies and interfingers with Killara Formation (Dawes and Pirajno 1998); unconformable with Juderina and Doolgunna Formations; type locality given; argillaceous sedimentary rocks, black shale, marl, dolostone, and minor chert.||||||
27828|Maraloou Formation|62353|5|Briefly described|map legend|Proterozoic|Proterozoic|Geol. Prov: Yerrida Basin.||Of Mooloogool Subgroup, Yerrida Group.||Overlies Killara Formation.|Argillaceous dolomitic limestone and interbedded siltstone; minor thin bedded limestone and dolomite.|14-APR-11
27828|Maraloou Formation|63866|5|Briefly described|p165-p166|Orosirian|Orosirian|Yerrida Basin.Age is a Monazite date derived from Rasmussen and Fletcher, 2002. Hosts gossans with anomalous Cu, Pd, Ba and Zn.|1843 +/- 14 Ma |Mooloogool Subgroup|||Carbonaceous shale.|
27828|Maraloou Formation|64580|4|Described|map legend||Paleoproterozoic|Of Mooloogool Group. Siltstone, ferruginous shale, in part calcareous; basal intercalated tholeliitic basalt pillow lava, dolerite sills.||||||09-DEC-08
27828|Maraloou Formation|64772|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic|Of the Mooloogool Group. Age: 1.8Ga.||||||07-FEB-11
27828|Maraloou Formation|65408|5|Briefly described|pp82-83, p84 Fig.1.|Paleoproterozoic|Paleoproterozoic|||Unit in Mooloogool Subgroup.||Overlies Killara Formation.|Sequence of black shale, siltstone and calcareous units.|
27828|Maraloou Formation|65411|6|Mentioned|p89 Fig.1.|||||Unit in Mooloogool Subgroup.||||
27828|Maraloou Formation|65412|5|Briefly described|p98, p101 Fig.4.|Paleoproterozoic|Paleoproterozoic||||||Succession of argillaceous and silty sediments.|
27828|Maraloou Formation|65419|1|Redefined|p4 Fig.1, p19, p23, pp27-29.|Paleoproterozoic|Paleoproterozoic|Of Bunting et al.(1977); revised by Gee and Grey (1993) to mainly comprise the upper carbonate-rich succession and subsidiary shale outcrops in the vicinity of Maraloou Well; this revision (Occhipinti et al. 1997) includes the basal succession of black shales. Named after Maraloou Well. This study presents a composite type section; total thickness c.1000 m. Strata of this unit on northern Mount Bartle 1:100 000, and northeast Glengarry 1:250 000, sheets are assigned in this study to the Thaduna Formation.||Unit in Mooloogool Subgroup.||Interfingers with/conformably overlies underlying Bartle Member. Overlies Killara Formation, Thaduna and Doolgunna Formations. Is unconformably overlain by Yelma Formation.|Argillaceous sediment, black shale, marl, dolostone and minor chert; local thin beds of graded quartz wacke; lower part comprises laminated carbonaceous argillite with carbonate nodules to 50 cm diameter; sulfides locally abundant.|
27828|Maraloou Formation|65472|5|Briefly described|p1, p2, p3 Fig.2, p4, p6, p9 Fig.8|||Thickness: 1000m. Yerrida Basin, well developed in southern parts. Age: U-Pb dating of monazite (from peperite margins of interfingering Maralou Formation and Killara Formation) (Rasmussen and Fletcher, 2002); considered a minimum depositional age for Maralou Formation and, by inference, provides a maximum age limit for deposition of overlying Yelma Formation. Also shown on p16, p17 Fig.15a.|c. 1.84 Ga|at top of Mooloogool Group||Interfingers with Killara Formation; is overlain disconformably/unconformably by Yelma Formation.|laminated siltstone, sulfidic and graphitic shale, marl, dolostone, and minor chert; intercalated basalt and dolerite near top.|
27828|Maraloou Formation|65913|3|Fully described|p2 Fig.1, pp17-19. |Paleoproterozoic|Paleoproterozoic|Covers much of the flat plain in the southwestern map area. Outcrops very poorly; there is no type section, but a type locality at Mount Russell. In the southwest map area, the rocks are locally steeply dipping; possibly due to surface creep, or localised block tilting or faulting. Surface weathering has produced calcrete in the southern map area. Black argillites are locally anomalous in Cu (up to 2800 ppm), Zn and Hg.||Unit in Mooloogool Subgroup.||Overlies Doolgunna, Thaduna and Killara Formations. Is unconformably overlain by Earaheedy Group.|Black shale; argillaceous dolomitic marlstone, massive to flaggy, pink to purple-brown, and interbedded siltstone; thin beds of dolomite and limestone; scour and fill; turbidite beds of medium- to coarse-grained quartz wacke trending northwards.|
27828|Maraloou Formation|66427|5|Briefly described|p41 Tb.1, p50|||Deposition of lake sediments. U-Pb monazite age (Rasmussen and Fletcher, 2002).|1843+/-14 Ma.|Of the Earaheedy Group.||||
27828|Maraloou Formation|67855|5|Briefly described|p204 tab 3-1, p206, 208|Paleoproterozoic|Paleoproterozoic|Gascoyne Complex, Nabberu Basin. 250m thick shale-carbonate-shelf facies. Shown as Maraloou Shale p208.||Glengarry Group||||
27828|Maraloou Formation|68055|5|Briefly described|p77-80|||Yerrida Basin.||Mooloogool Group.||Is overlain by (outliers of) Yelma Formation.|Includes pyritic black shales.|
27828|Maraloou Formation|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic|||Mooloogool Group|||siltstone, ferruginous shale, in part calcareous; basal intercalated tholeliitic basalt pillow lava, dolerite sills|
27828|Maraloou Formation|69003|4|Described|p11-13, p26|||Yerrida Basin. c.1000m thick. Intruded by mafic sills c.1840 Ma.|c.1840 Ma.|Mooloogool Group.||Conformably overlies Doolgunna, Thaduna and Killara Formations.|Finely laminated argillite and sulfidic shales; contains peperite.|
27828|Maraloou Formation|69152|5|Briefly described|500k_geologyp08_lut||Paleoproterozoic|||Mooloogool Group|||Siltstone, ferruginous shale, in part calcareous; basal intercalated tholeliitic basalt pillow lava, dolerite sills.|06-AUG-15
27828|Maraloou Formation|70153|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic||2500 - 1600 Ma (inferred).|Mooloogool Group|||Siltstone, ferruginous shale, in part calcareous; basal intercalated tholeliitic basalt pillow lava, dolerite sills.|
27828|Maraloou Formation|70795|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|West Australian Craton, Yerrida Basin|2500-1600 Ma||||Siltstone, ferruginous shale, in part calcareous; basal intercalated tholeiitic basalt pillow lava, dolerite sills.|
27828|Maraloou Formation|70796|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|Yerrida Basin, Capricorn Orogen. Misspelt as the Maralou Formation in glengarry_100k_geologyp_lut.csv, glengarry_500k_interpgeop_lut.csv.|ca 25001600 Ma (inferred)|Mooloogool Group|||Siltstone, ferruginous shale, in part calcareous; basal intercalated tholeliitic basalt pillow lava, dolerite sills.|
27828|Maraloou Formation|70804|6|Mentioned|p2, p37|||Previously of the Glengarry Group.||Mooloogool Subgroup||||
27828|Maraloou Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, shale, marl, sedimentary breccia|
27828|Maraloou Formation|71269|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Of Yerrida Basin. Events: Capricorn Orogeny (1817-1772 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, glengarry_100k_geologyp_lut.csv, glengarry_500k_interpgeop_lut.csv.|2170-1600 Ma (inferred)|Unit of Mooloogool Group.|||Siltstone, ferruginous shale, in part calcareous; basal intercalated tholeliitic basalt pillow lava, dolerite sills|
27828|Maraloou Formation|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: West Australian Craton. Events: Capricorn Orogeny (1817 - 1772 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv.|2170-1600 Ma (inferred)||||Siltstone, ferruginous shale, in part calcareous; basal intercalated tholeliitic basalt pillow lava, dolerite sills|
27828|Maraloou Formation|71468|4|Described|p24-26|Orosirian|Orosirian|Geological province: Capricorn Orogen, Yilgarn Craton. Of Yerrida Basin. Monazite at base of formation dated at 1843+\-10 Ma (Rasmussen and Fletcher, 2002), interpreted to represent low-grade metamorphic overprint rather than contact metamorphism related to mafic sills.||Unit of Mooloogool Group.||Overlain by Tooloo Group. Underlain by, and grades into Killara Formation.|Siltstone and ferruginous shale; the latter is calcareous in parts.|
27828|Maraloou Formation|71484|4|Described|p123-125,128,134,136|||Geological province: Of Yerrida Basin. Contains monazite samples dated at 1843+\-14 Ma, in contact with subvolcanic dolerites sills of the Killara Formation (peperite contacts), interpreted to constrain a minimum depositional age, ans indicating partly coeval deposition. Represents the end of basin-fill and volcanism in the Mooloogool Sub-basin in a lacustrine depositional environment. Inboard correlative to the Horseshoe Formation.||Unit of Mooloogool Group.||Uppermost unit of Mooloogool Group. Overlain unconformably by Yelma Fm and Sweetwaters Well Dolomite. Underlain by Doolgunna and Thaduna Formation.|Siltstone, ferruginous shale, in part calcareous, basal part intercalated with basaltic volcanics and dolerite sills.|30-AUG-19
27828|Maraloou Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Yerrida Basin.||Mooloogool Group|||Siltstone, ferruginous shale, in part calcareous; basal intercalated tholeliitic basalt pillow lava, dolerite sills.|
28204|Marble Bar Chert Member|23783|5|Briefly described|p14|Archean|Archean|See also p98.||||||07-NOV-08
28204|Marble Bar Chert Member|24184|5|Briefly described|p699, 700|Archean|Archean|Of the Talga Talga Subgroup. Geological Province: Pilbara Craton. Age: ca.3460Ma. Formerly correlated as part of Towers Formation, now a distinct unit (Van Kranendonk 2000).||||||07-NOV-08
28204|Marble Bar Chert Member|24590|5|Briefly described|p130 Fig.4.1|Archean|Archean|Middle member of the Towers Formation. Max. thickness: 100m.||||||07-FEB-11
28204|Marble Bar Chert Member|31309|1|Redefined|p53|Archean|Archean|||||||07-NOV-08
28204|Marble Bar Chert Member|38498|6|Mentioned|p60|||||||||
28204|Marble Bar Chert Member|39697|6|Mentioned|p23|||See also p53.||||||14-JAN-22
28204|Marble Bar Chert Member|43595|5|Briefly described|p213|||||||||
28204|Marble Bar Chert Member|44150|5|Briefly described|p133 Tb.2-16|||Distinctive ridge-forming unit, 100 m thick.||Towers Formation|||Red and white, or grey and white banded chert.|
28204|Marble Bar Chert Member|61111|6|Mentioned|p96 Fig.2|||||||||
28204|Marble Bar Chert Member|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Geological Province: eastern Pilbara Craton.||||||07-NOV-08
28204|Marble Bar Chert Member|63245|5|Briefly described|p4 Fig. 1|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Geological Province: Pilbara Craton.||||||07-NOV-08
28204|Marble Bar Chert Member|63420|5|Briefly described|Map legend|Archean|Archean|Of the Duffer Formation (Coongan Subgroup, Warrawoona Group, Pilbara Supergroup). Geological Province: Pilbara Craton. Red, white and grey layered chert; metamorphosed.||||||07-NOV-08
28204|Marble Bar Chert Member|63441|5|Briefly described|p4 Tb. 1, p20|Archean|Archean|Redefined as part of the Duffer Formation (Coongan Subgroup, Warrawoona Group, Pilbara Supergroup). Formerly of the Towers Formation. Geological province: Pilbara Craton.||||||07-FEB-11
28204|Marble Bar Chert Member|64405|5|Briefly described|p6, p15|||Of Lowe (1983). See also p4 Fig. 3.||||||07-FEB-11
28204|Marble Bar Chert Member|64621|5|Briefly described|Map legend|Archean|Archean|Of Duffer Formation (Coongan Subgroup, Warrawoona Group). Red, white and grey layered chert; metamorphosed.||||||07-NOV-08
28204|Marble Bar Chert Member|64747|6|Mentioned|p94 fig 1, p119|||||Duffer Formation||||
28204|Marble Bar Chert Member|64936|5|Briefly described|map legend|Archean|Archean|Of Towers Formation. Under Apex Basalt, over Duffer Formation. Chert, weakly metamorphosed. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
28204|Marble Bar Chert Member|65827|6|Mentioned|p19|||Thin-bedded cherts in the basal Apex Basalt may be facies equivalents to this Member.||||||21-JAN-22
28204|Marble Bar Chert Member|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Member of Duffer Formation. Red, white and grey layered chert; metamorphosed.||||||
28204|Marble Bar Chert Member|66217|5|Briefly described|p5, p17, p19, pp21-24, p60.|||East Pilbara Terrane, Pilbara Craton. These rocks were originally part of the Towers Formation (Hickman 1977); re-assigned to the Duffer Formation by Van Kranendonk et al. (2006a). Hosts a silica prospect, and is cut by barite veins, in the Warralong greenstone belt. ||Unit in Duffer Formation.||Is overlain by Panorama Formation.|Millimetre- to centimetre-thick layers of  red, white and black cherts; locally includes fine-grained, clastic sedimentary rock.|
28204|Marble Bar Chert Member|66664|6|Mentioned|p9.|||||Unit in Duffer Formation.||||
28204|Marble Bar Chert Member|66745|6|Mentioned|p54 Fig.4.|Paleoarchean|Paleoarchean|||Unit in Duffer Formation.||||
28204|Marble Bar Chert Member|67130|5|Briefly described|p16, p53, p58|Paleoarchean|Paleoarchean|Layering at millimetre to centimetre scale suggestive of deposition under quiet water, deep marine conditions.|c. 3470 Ma|Duffer Formation||Overlies Duffer Formation, Mount Ada Basalt, overlain by Apex Basalt|Jaspilitic chert, blue black chert, white chert|
28204|Marble Bar Chert Member|67197|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Duffer Formation.||||
28204|Marble Bar Chert Member|67269|5|Briefly described|p6 Fig.3|Paleoarchean|Paleoarchean|||Duffer Formation.||Is overlain by Apex Basalt.|Jaspilite.|
28204|Marble Bar Chert Member|67270|5|Briefly described|p4-6, p9-10, p18, p21-22, p26, p29|Paleoarchean|Paleoarchean|Van Kranendonk et al. (2001). Marble Bar vicinity, East Pilbara Terrane. Photographs, photomicrographs.||Duffer Formation.|||Finely laminated layers of red jaspilitic (hematite-rich) chert containing thin lenses and alternations of white cryptocrystalline chert; crosscut, displaced or replaced by veins of black-and-white chert.|
28204|Marble Bar Chert Member|68035|5|Briefly described|p288 Fig 4|Paleoarchean|Paleoarchean|Warrawoona Group, Pilbara Supergroup, East Pilbara Terrane.||Near or at top of Duffer Formation|||Jaspilite.|
28204|Marble Bar Chert Member|68280|5|Briefly described|p2, p4, p27, p30, p32, p33, p35|||||Duffer Formation|||150m Thick. Jaspilite and siliciclastic rocks, thinly bedded jasper. Intruded by dolerite sill.|
28204|Marble Bar Chert Member|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|Age contrained by the parent Duffer Formation.|3471-3463 Ma (parent)|Of the Duffer Formation.|||Red-, white-, and grey-layered chert (metamorphosed).|11-JUN-14
28204|Marble Bar Chert Member|68283|5|Briefly described|Map Legend|Archean|Archean|East Pilbara Terrane, Pilbara Craton. Age inferred from parent unit.||Of the Duffer Formation.|||Red, white, and grey layered chert; metamorphosed.|23-SEP-13
28204|Marble Bar Chert Member|68284|5|Briefly described|p7|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Duffer Formation.||Is overlain by Apex Basalt.||
28204|Marble Bar Chert Member|69012|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|||Of the Duffer Formation.|||Comprises red, white, and grey layered chert; metamorphosed.|
28204|Marble Bar Chert Member|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. ||Of the Duffer Formation.|||Jaspilitic chert; metamorphosed.|02-MAY-14
28204|Marble Bar Chert Member|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Duffer Formation|||Red-, layered chert and jaspilitic chert; metamorphosed|
28204|Marble Bar Chert Member|69301|5|Briefly described|p5 Fig.3, p10|||Pilbara Craton. East Pilbara Terrane.||Duffer Formation||||
28204|Marble Bar Chert Member|69569|6|Mentioned|p285 Fig.2|||East Pilbara Terrane. See also reference to Marble Bar Chert (p288).||||||
28204|Marble Bar Chert Member|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv.|3463 Ma (inferred)|Unit of Duffer Formation.|||Red-, white- and grey-layered chert; jaspilitic, metamorphosed|
28204|Marble Bar Chert Member|70733|5|Briefly described|p103-108, 111, 114, 116-120|||East Pilbara Craton. Abbreviated to Marble Bar Chert Member after the first one or two mentions. Previously named Towers Formation.  Contains a newly-discovered impact ejecta unit (described in detail). Type section is along the Coongan River; type area is at Marble Bar Pool, 3km WSW from Marble Bar town where it is 60m thick; steeply overturned. Extends over ~10,000 km2. Drill hole section. Photomicrographs. Whole-rock analytical data tabulated. PGE values compared with other ejecta units.|Between 3459 +/- Ma and 3449 +/- 3 Ma.|Uppermost Duffer Formation.||Is overlain by Apex Basalt.|Dark grey chert; spectacularly variegated red and white banded chert; mainly composed of silicified fine-grained clastic sediments and tuffaceous material. Includes layers with 1-2mm diameter silica-dominated spherules.|
28204|Marble Bar Chert Member|70884|5|Briefly described|p123|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Coongan Subgroup.||Overlain unconformably by Apex Basalt/Salgash Subgroup. Underlain by Duffer Formation.||
28204|Marble Bar Chert Member|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Warrawoona  Large Igneous Province.||Duffer Formation|||Layered grey, red, and white chert; metamorphosed.|
28204|Marble Bar Chert Member|72064|5|Briefly described|p66|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Dufer Formation.||Overlain unconformably by Panorama Formation or Apex Basalt.||28-JAN-20
28204|Marble Bar Chert Member|72668|6|Mentioned|p5 Fig.3|||Of Duffer Formation? Figure not clear.||||||
23763|Marboo Formation|22474|6|Mentioned|p21|Orosirian||||||||
23763|Marboo Formation|22526|6|Mentioned|Fig2 P681, Fig3||Orosirian|||||||
23763|Marboo Formation|22547|3|Fully described|p9||Orosirian|Within the Lamboo Complex, Halls Creek Orogen. Age: 1870 Ma.||||||01-DEC-06
23763|Marboo Formation|22716|5|Briefly described|table4, p232|Orosirian|Orosirian|Age: 1870Ma||||||
23763|Marboo Formation|22754|4|Described|p6|Paleoproterozoic|Paleoproterozoic|Of the Lamboo Complex.  Previously correlated with Olympio Formation.  Intruded by Paperbark supersuite.||||||07-NOV-08
23763|Marboo Formation|23323|5|Briefly described|p454 Fig.2|Orosirian|Orosirian|Age: 1870-1865 Ma.||||||07-FEB-07
23763|Marboo Formation|23383|4|Described|p7, p5 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Lamboo Complex. Variably deformed and metamorphosed interbedded mudstone, siltstone, greywacke and quartz wacke. Age: 1870 Ma.  Max. thickness: >700m (on LENNARD RIVER sheet). See also p6 Fig. 3, and p8-9.||||||22-DEC-08
23763|Marboo Formation|23601|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Low grade turbiditic metasandstone; quartz-chlorite-muscovite phyllite; narrow zones of medium to high grade quartz-muscovite-biotite-andalusite-cordierite hornfels occur adjacent to granitoid intrusions.Age: >1880Ma.||||||07-NOV-08
23763|Marboo Formation|23621|4|Described|p20|Orosirian|Orosirian|See also page 11 table 1. Previously mapped as Ticklara Metamorphics. Age: ~1872 Ma. Geological Province: Halls Creek Orogen.||||||
23763|Marboo Formation|23622|5|Briefly described|Map Legend|Orosirian|Orosirian|||||||
23763|Marboo Formation|23722|4|Described|p5|Paleoproterozoic|Paleoproterozoic|Thinly bedded metamorphosed turbidites. Equivalent of Olympia Formation defined in the Halls Creek Orogen. Geological Province: Hooper Complex.||||||22-DEC-08
23763|Marboo Formation|23751|6|Mentioned|p8|Orosirian|Orosirian|Age. c.1870 Ma.||||||
23763|Marboo Formation|23925|5|Briefly described|p220 Fig. 2|Orosirian|Orosirian|Age: c. 1870-1865 Ma. Geological Province: Halls Creek Orogen.||||||
23763|Marboo Formation|24173|4|Described|p16, p20|Paleoproterozoic|Paleoproterozoic|Unconformably overlain by Whitewater Volcanics. Geological Province: Halls Creek Orogen. Forms part of the Mount Joseph Migmatite. Age: c.1872Ma. Intrudud by Lennard Granite. Possible correlative is Milba Formation||||||07-NOV-08
23763|Marboo Formation|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Low- to high-grade, metamorphosed turbiditic sandstone and siltstone, and mudstone; hornfelsed adjacent to granitoid intrusions.  Age: 1870Ma.||||||07-NOV-08
23763|Marboo Formation|24572|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Metamorphosed sedimentary rocks.  Age: >1835Ma.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
23763|Marboo Formation|42710|5|Briefly described|map legend|Proterozoic||||||||
23763|Marboo Formation|42811|3|Fully described|p5|||Of Hooper Complex.||||||09-DEC-08
23763|Marboo Formation|42814|3|Fully described|p5|||||||||
23763|Marboo Formation|42815|5|Briefly described|map|||||||||
23763|Marboo Formation|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|Approx 1870-1865 Ma.||||||
23763|Marboo Formation|43561|6|Mentioned|p1436|||Deposited at approx. 1870 Ma||||||
23763|Marboo Formation|43666|5|Briefly described|p6,8,52 Table 2|Proterozoic|Mesoproterozoic|||||||
23763|Marboo Formation|43803|6|Mentioned|fig.3,p69||Precambrian|||||||
23763|Marboo Formation|43819|5|Briefly described|p33||Paleoproterozoic|Biotite age: 700+/-8 Ma||||||07-NOV-08
23763|Marboo Formation|43853|5|Briefly described|Map Legend||Proterozoic|||||||
23763|Marboo Formation|43854|5|Briefly described|Map Legend||Proterozoic|Of Lamboo Complex.||||||22-DEC-08
23763|Marboo Formation|43931|6|Mentioned|p21|||Halls Creek Province||||||
23763|Marboo Formation|44230|5|Briefly described|Map Legend||Proterozoic|||||||
23763|Marboo Formation|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Metamorphosed low-grade turbiditic sandstone, and quartz-chlorite-muscovite phyllite; includes narrow zones of quartz-muscovite-biotite-andalusite-sillimanite-cordierite-K-feldspar-hornfels adjacent to granitic intrusions. Age: c.1870Ma.||||||07-NOV-08
23763|Marboo Formation|44694|5|Briefly described|Map Legend||Proterozoic|||||||
23763|Marboo Formation|44868|5|Briefly described|Map Legend||Proterozoic|||||||
23763|Marboo Formation|50437|6|Mentioned|p2.1, 3.4|||Intruded by: Paperbark Supersuite.||||||
23763|Marboo Formation|60283|6|Mentioned|p25 Fig.2|||Halls Creek Orogen.||||||
23763|Marboo Formation|60533|5|Briefly described|p593|Paleoproterozoic|Paleoproterozoic|Age:1900-1865Ma. Geological Province: Halls Creek Orogen.||||||07-NOV-08
23763|Marboo Formation|60724|4|Described|p15, p5 Fig. 2|||Turbiditic sequence of thinly bedded metamorphosed mudstone, siltstone and quartz wacke. Unconformably overlain by Speewah and Kimberley Formations. ||||||
23763|Marboo Formation|63866|4|Described|p129, p132|||Western Zone, Halls Creek Orogen. Interpreted to represent a submarine fan system with palaeo-current data indicating sediment transport from the north and northeast. Thought to be the unmetamorphosed equivalent of the Amherst Metamorphics and the Mount Joseph migmatite.|<1872 Ma (Tyler et al, 1999)|||Unconformably overlain by the Whitewater Volcanics.|Turbiditic sandstone, greywackes and mudstones.|
23763|Marboo Formation|64572|5|Briefly described|p802 Fig. 4, p803 Fig. 5|Paleoproterozoic|Paleoproterozoic|Age: ~1870Ma. Geological Province: Kimberley Craton. Basement sedimentary rocks.||||||22-DEC-08
23763|Marboo Formation|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Low- to high-grade, metamorphosed turbiditic sandstone and siltstone, and mudstone; hornfelsed adjacent to granitoid intrusions.||||||09-DEC-08
23763|Marboo Formation|64722|5|Briefly described|Fig. 2 p3-6, p9|Orosirian|Orosirian|Of Halls Creek Orogen. A cratonic margin accumulation located along the southern and southwestern margins of the Kimberley Block.||||||
23763|Marboo Formation|64730|5|Briefly described|p141|Paleoproterozoic|Paleoproterozoic|Ruins Dolerite intrusion prior to regional deformation. ?intruded by Richenda Microgranite(~1858 Ma) post-deformation.|Max. deposition age 1871 +/- 9 Ma.|||Intruded by Ruins Dolerite. Unconformably overlain by the Whitewater Volcanics.|Turbiditic deformed metasediments.|02-MAY-12
23763|Marboo Formation|64731|5|Briefly described|p164|Paleoproterozoic|Paleoproterozoic|In Hooper Complex of Halls Creek Orogen.||||||12-APR-12
23763|Marboo Formation|64956|5|Briefly described|p2 Tb. 27, p96-97|Paleoproterozoic|Paleoproterozoic|Max. depositional age: 1871+/-4Ma. Geological province: Halls Creek Orogen. Sample is chloritic meta-siltstone (fine-grained) from a unit mapped as Halls Creek Group now interpreted to be Marboo Formation.||||||07-FEB-11
23763|Marboo Formation|66845|5|Briefly described|p536 Fig.2|Paleoproterozoic|Paleoproterozoic|Western zone of Lamboo Complex|1870-1863 Ma|||||
23763|Marboo Formation|66846|5|Briefly described|p549 Fig.2, p560|Orosirian|Orosirian|Underlies Ruins Dolerite. In the Western Zone of the Lamboo Complex.|||||Turbidite.|
23763|Marboo Formation|68078|5|Briefly described|p5, p19|Paleoproterozoic|Paleoproterozoic|Age is maximum depositional age.|1872 Ma|||Unconformably overlain by Whitewater Volcanics, Speewah Group, intruded by Paperbark Supersuite|Interbedded turbiditic quartz wacke, siltstone and mudstone.|07-SEP-22
23763|Marboo Formation|69003|4|Described|p5, p18-19|||W zone of the Lamboo Province, Halls Creek Orogen. Underwent medium- to high-grade metamorphism during the c.1860 Ma Hooper Orogeny.|c.1872 Ma (maximum depositional age).|||Is overlain by Whitewater Volcanics. Intruded by the Paperbark Supersuite.|Interbedded fine- and medium-grained turbidites.|
23763|Marboo Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Oldest unit of Lamboo Province, Halls Creek Orogen. Age from data released June 2013, geochron file 206102.1.pdf. Note: rocks at geochron sampling site were originally assigned to Halls Creek Group (Derrick & Playford, 1973), then Olympio Formation (Geoscience Australia, 2012).|Conservative max.deposit 1983+/-9 Ma U/Pb SHRIMP||Includes 3 unnamed members.|Unconformably overlain by Speewah and Kimberley Basin rocks.|Predominantly low grade, thin-bedded turbiditic metasandstone and quartz-chlorite-muscovite phyllite; hornfelsed adjacent to granite intrusions.|03-AUG-15
23763|Marboo Formation|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv. |||||Low grade, thinly bedded turbiditic metasandstone and quartz-chlorite-muscovite phyllite. Medium grade psammite and pelite; quartz-muscovite-sillimanite-andalusite schist. Granofels, hornfels and hornfelsic schollen migmatite.|
23763|Marboo Formation|69417|6|Mentioned|p2:5|Orosirian|Orosirian|Halls Creek Orogen.||||||12-JUL-16
23763|Marboo Formation|69422|5|Briefly described|p7:1-3|Orosirian|Orosirian|Griffin et al. (1993). Western Zone, Halls Creek Orogen. Deformed, metamorphosed and intruded during the 1865-1850 Hooper Orogeny. Originally mapped as Halls Creek Group by Whitehead and Fahey (1985) and Dunster et al. (2000); identified by extrapolation from WA as "almost certainly" Marboo Formation. Maximum depositional age of 1871 +/- 4 Ma (Worden et al., 2008), effectively identical with c.1872 Ma by Tyler et al. (1999) in WA.|< c.1871 Ma.|||Is overlain unconformably by Whitewater Volcanics.|Low- to high-grade metasedimentary turbiditic rocks: a succession of ferruginous, fine-grained, greenschist facies phyllite and schist; rare evidence of compositional layering.|12-JUL-16
23763|Marboo Formation|69585|5|Briefly described|p2, p4, p27|Orosirian|Orosirian|Western Lamboo Province.|1870 Ma.|||Is intruded by Paperbark Supersuites.|Metasedimentary rocks.|
23763|Marboo Formation|69597|5|Briefly described|p3, p5, p68|Paleoproterozoic|Paleoproterozoic|Western Lamboo Province. |c. 1870 Ma|||Intruded by the Paperbark Supersuite.|Turbiditic metasedimentary rocks.|
23763|Marboo Formation|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Oldest rock unit in the Lamboo Province.Ssequence of turbiditic metasedimentary rocks with paleocurrent directions implying derivation from the northwest in an area of crust now buried beneath the unconformably overlying Speewah and Kimberley Basins (Hancock, 1991; Tyler et al., 1999). Interpreted maximum depositional age of 207Pb/206Pb* date of 1846+\-20 Ma (weighted mean date of 1876+\-4 Ma). Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 250k_geologyp_lut.csv, 500k_interpgeop_lut.csv, 250k_interpgeop_lut.csv and geochron files.|1872-1864 Ma (Inferred)||||Thin-bedded, turbiditic metasandstone, psammite and quartz-chlorite-muscovite phyllite; granofels, hornfels, and hornfelsic schollen (raft) migmatite|
23763|Marboo Formation|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Kimberley Craton.|1872 - 1864 Ma; Tyler et al. (1999).||||Thin-bedded, turbiditic metasandstone and quartz-chlorite-muscovite phyllite; hornfelsed adjacent to granite intrusions.|
23763|Marboo Formation|69673|6|Mentioned|p3 fig 2|Orosirian|Orosirian|||||||
23763|Marboo Formation|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province; Halls Creek Orogen; North Australian Craton.|>1872 Ma (Tyler et al., 1999).||||Thin-bedded, turbiditic metasandstone and quartz-chlorite-muscovite phyllite; hornfelsed adjacent to granite intrusions.|
23763|Marboo Formation|70154|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 250k_interpgeop_lut.csv. |1864-1872 Ma||||Thin-bedded, turbiditic metasandstone and quartz--chlorite--muscovite phyllite; hornfelsed adjacent to granite intrusions, psammitic and pelitic schist, quartz-muscovite-biotite psammite and pelite.|
23763|Marboo Formation|70731|5|Briefly described|p267-269,272-273,278|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. Likely formed in a post-collisional setting (Griffin et al., 2000) and underwent low-to high-grade metamorphism during Hooper Orogeny (1865-1850 Ma). Emplacement of c. 1857 Ma Springvale and c. 1855 Toby layered mafic intrusions at 8-18km depth coinciding with Hooper Orogeny.|c. 1872 Ma|||Overlain by Whitewater Volcanics.||
23763|Marboo Formation|70812|4|Described|p3, p6-p8, p10, p19, p25, p27, p30|Paleoproterozoic|Paleoproterozoic|Western Zone of the Halls Creek Orogen, Lamboo Province. Deformed and metamorphosed at low to high grade during the 1870-1850 Hooper Orogeny. Mineralisation is described.|c. 1870 Ma (Maximum depositional age)|||Overlain by the Whitewater Volcanics. Intruded by the Paperbark Supersuite. Partially equivalent to the Amhurst Metamophics.|Turbiditic rocks.|
23763|Marboo Formation|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|||||||
23763|Marboo Formation|70851|5|Briefly described|p3-p5, p11-p12, p24, p29, p34|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province. This unit underwent low- to high-grade metamorphism during the Hooper Orogeny. Rock properties are provided.|c. 1872 Ma||||Turbiditic sedimentary rocks.|
23763|Marboo Formation|71113|4|Described|p96,99|Orosirian|Orosirian|Geological province: Western Zone, Lamboo Province, Halls Creek Orogen. Deposited along the rifted margin of the Kimberley Craton (Griffin et al., 2000; Tyler et al., 1999). Intruded by Paperbark Supersuite, and other potassic I-type granitic and subvolcanic rocks between 1865-1850 Ma.|c. 1870 Ma|||Overlain unconformably by Whitewater Volcanics.|Turbiditic sandstone, siltstone, greywacke, and quartz wacke.|
23763|Marboo Formation|71140|6|Mentioned|p96, 99|Orosirian|Orosirian|Western Zone, Lamboo Province, Halls Creek Orogen. Deposited along rifted margin of the Kimberley Craton.|c.1870 Ma.|||Is overlain unconformably by Whitewater Volcanics. Is intruded by Paperbark Supersuite.|Turbiditic sandstone, siltstone, greywacke and quartz wacke.|
23763|Marboo Formation|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Oldest rock in the Lamboo Province. Paleocurrent directions imply derivation from NW, an area of crust now buried beneath the unconformably overlying Speewah and Kimberley Basins (Hancock, 1991; Tyler et al., 1999). Underwent contact metamorphism associated with granites of the Paperbark Supersuite. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyp_lut.csv, 1m_interpgeop_lut.csv and geochron files.|1872-1864 Ma (inferred)||Includes Mount Joseph Migmatite.|Intruded by Richenda Microgranodiorite and Ruins Dolerite.|Thin-bedded, turbiditic metasandstone and quartz-chlorite-muscovite phyllite; hornfelsed adjacent to granite intrusions, granofels, hornfels, and hornfelsic schollen (raft) migmatite, medium-grade psammitic and pelite and pelitic schist.|
23763|Marboo Formation|71281|5|Briefly described|p421-422, p431-432|Paleoproterozoic|Paleoproterozoic|Lamboo Province. Deformed during the 1870-1850 Ma Hooper Orogeny.|< c.1872 Ma.|||Is intruded by the Paperbark Supersuite.|Metagreywackes.|
23763|Marboo Formation|71397|4|Described|p2,5|Orosirian|Orosirian|Geological province: Western Zone, Lamboo Province, Halls Creek Orogen. Oldest exposed rocks in the Western Zone, Lamboo Province. Metasedimentary rocks metamorphosed to greenschist and overprinted by layer-parallel foliation during D1/M1 Hooper Orogeny at 1870-1864 Ma (Tyler et al., 1999; Griffin et al., 2000a); metamorphosed to greenschist and granulite facies before and during Paperbark Supersuite intrusion. Tyler et al. (1999) reported a maximum depositional age of 1872+\-9 Ma from a metasandstone sample. Subdivided into upper and lower sections, of middle fan and upper fan depositional environments respectively (see p2 for references).||||Intruded by Ruins Dolerite and Paperbark Supersuite.|Metamorphosed quartzofeldspathic greywacke with lesser metasiltstone and metamudstone, overlain by beds of metamudstone and metasiltstone with lesser metamorphosed quartzofeldspathic greywacke.|
23763|Marboo Formation|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen, North Australian Craton.|<1872 - 1864 Ma.||||Thin-bedded, turbiditic metasandstone and quartz-chlorite-muscovite phyllite; hornfelsed adjacent to granite intrusions. A subunit of migmatite and gneisses is mapped separately.|
23763|Marboo Formation|71873|5|Briefly described|p426,444|Orosirian|Orosirian|Geological province: Lamboo Province. Turbiditic passive margin metasedimentary succession.|1872+\-9 Ma|||Intruded by Ruins Dolerite sills and Paperbark Supersuite.||
23763|Marboo Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Central Zone, Halls Creek Orogen.|||Includes Mount Joseph Migmatite.||Thin-bedded, turbiditic metasandstone and quartz--chlorite-muscovite phyllite; hornfelsed adjacent to granite intrusions.|
23763|Marboo Formation|72437|5|Briefly described|p13-15|||Interpreted to be overprinted by a high-grade metamorphic event between 1860 Ma and 1820 Ma. A single whole rock analysis is presented of a cordierite-biotite syenogranite interpreted to be an anatectic S-type melt derived from turbidites of the Marboo Formation.||||Equivalent to the Mount Joseph Migmatite.|Turbidites.|
23763|Marboo Formation|72490|6|Mentioned|p3-4|Orosirian|Orosirian|Lamboo Province. Age is detrital zircon maximum depositional age.|ca. 1872 Ma|||Overlain by Whitewater Volcanics. Intruded by Paperbark Supersuite.|Greenschist to granulite facies turbiditic metasedimentary rocks.|
23763|Marboo Formation|73089|6|Mentioned|p32-33, p36|Orosirian|Orosirian|Lamboo Province, Western Zone. [Referred to as Lower Marboo Formation and Upper Marboo Formation on p32 and upper Marboo Formation on p33]. Dominantly Paleoproterozoic detritus. Paleocurrent indicators have been measured from this unit, indicating south- and southwest-dipping paleoslopes.|c. 1875-1855 Ma||||Includes metasedimentary units.|
33915|Marcia Bore gneiss|22449|6|Mentioned|Table3 P27||Archean|Age of unit is 3115 Ma||||||07-NOV-08
68513|Mardeburra Granodiorite|63441|2|Defined|p10 Tb. 2, p37|Archean|Archean|Of the Sisters Supersuite.  Age: <3006+/-12Ma. Forms most easterly part of Cherratta Granitic Complex. Unconformable below Hardey Fm. Geological province: Pilbara Craton. (discrepancy here - Table 2 p10 puts this into Maitland River Supersuite)???||||||07-FEB-11
68513|Mardeburra Granodiorite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Maitland River Supersuite. Geological province: Pilbara Craton.  Porphyritic biotite granodiorite; foliated and weakly banded; intruded by pegmatitic leucocratic microgranite; metamorphosed.||||||07-NOV-08
68513|Mardeburra Granodiorite|70775|5|Briefly described|p16, p53-p54|||Over 50 percent of zircon dated in this unit are older than 3100 Ma. Together with the Jean Well Granodiorite, Whyjabby Granodiorite, Brill Monzogranite, Waloo Waloo Monzogranite and Toorare Tonalite comprises the Cherratta Granitic Complex.|c. 3006 +/- 12 Ma|Maitland River Supersuite|||Porphyritic biotite granodiorite.|
77946|Maria Mine Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2690 - 2660 Ma (inferred).|Mount White Group|||Includes sandstone and conglomerate with common granitic and mafic clasts; metamorphosed. Sandstone, conglomerate, siltstone, shale, and chert; metamorphosed; locally deeply weathered|
77946|Maria Mine Formation|71212|5|Briefly described|intro p2|||Yilgarn Craton. Equivalent to the informal Maria metasediments. ||Mount White Group||||
77946|Maria Mine Formation|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2692-2662 Ma (inferred)|Unit of Mount White Group.|||Sedimentary rock, undivided; includes sandstone, conglomerate, siltstone, shale, and chert; common granitic and mafic clasts, metamorphosed; locally deeply weathered|
77946|Maria Mine Formation|73151|4|Described|p1-3, p5-6, p8, p9 Fig.5, p11-13, p15-16|Neoarchean|Neoarchean|Yilgarn Craton, Kalgoorlie Terrane. Upper part of the Mount White Group. Appears to be conformable with the Vivien Formation, upper and lower bounding contacts do not outcrop. Low-energy depositional environment of ring-plain surrounding a volcanic island, water depth of at least 50m, interrupted by episodic mass flows, turbidites. Conglomerate clasts derived from upper units of the Kalgoorlie Group (Turret Dolerite, White Hope Basalt, Redeemer Basalt, Burrell Well Basalt) reflect a slightly deeper level of erosion than inferred from the underlying Vivien Formation. Interdigitated coherent mafic to intermediate magmatic rocks are predominantly intrusive, includes Halfway Well Basalt. Location in text includes p14 Fig.9.|ca. 2670-2665 Ma|Mount White Group||Conformably overlies Vivien Formation. Unconformably underlies Scotty Creek Formation.|Bedded mudstone, chert, sandstone and conglomerate. Include basaltic andesite. Massive, poorly sorted and clast-supported conglomerates contain rounded felsic clasts with medium- and plutonic groundmass textures, less common mafic clasts.|
77946|Maria Mine Formation|73596|5|Briefly described|p1152, 1157-1160, 1162|||Lawlers Domain, Agnew-Wiluna Greenstone Belt. Clasts derived from underlying Mount White Group and upper Two Sisters Subgroup.||Mount White Group.||Overlies Halfway Well Basalt, probably unconformably. Is overlain by Scotty Creek Formation. Correlated with Black Flag Group.|A dominant basal conglomerate (polymict, rounded pebble to cobble clasts, locally boulders); conformably overlain by a sequence of siltstones and argillites.|
22264|Mariginiup Member|12759|2|Defined|p35; p28 Tb. 7; p32 Fig 15; P36 Fig 17|Berriemian|Valanginian|New name. Rocks previously included in either South Perth Shale or Leederville Formation. Named from: Lake Mariginiup, Wanneroo. Type section: Bore AM24 between 423-507m depth (max 250 m) at AMG Zone 50, 389624m E, 6491151m N.||Basal Member of Leederville Formation.||Overlain by Wanneroo or Pinjar Members; underlain conformably (transitionally) by South Perth Shale or Gage Formation, and unconformably by Cattamarra Coal Measures, Yarragadee or Parmelia Formations|Thinly interbedded and discontinuous grey to black siltstones and shales, minor very thin beds of mostly fine-grained sandstone; predominantly marine; commonly glauconitic, micaceous, locally fossiliferous; variably pyritic or calcareous cemented.|12-MAY-14
22264|Mariginiup Member|67115|5|Briefly described|p63-4, p69-70 |Cretaceous|Cretaceous|Represents the lower confining aquiclude.  Thickness varies from 15 to 235 m. Lithology and trace elements detailed.||Basal unit in Leederville Formation.||Conformable transitional contacts with the overlying Wanneroo Member and underlying South Perth Shale.|Clay-silt and sands.|
22264|Mariginiup Member|68254|5|Briefly described|p1039, p1040 Tb.3, p1043, p1046 Tb.4|Cretaceous|Cretaceous|Identifiable by its characteristically high gamma ray logs.||Of the Leederville Formation|||Comprises macaceous and glauconitic marine siltstones and shales.|
37720|Marillana Formation|24573|4|Described|p685|Middle Miocene|Late Oligocene|Unconformably overlies the Hamersley Group. Disconformably overlain by calcretised carbonate equated with the Oakover Formation. Max Thickness: 120m. Geological Province: central Hamersley Range||||||
37720|Marillana Formation|60539|5|Briefly described|p498, 500 Fig.2, 501 Fig.3|Early Miocene|Late Eocene|Geological Province: Pilbara Craton. Includes: Munjina Member, Barimunya Member, Iowa Eastern Member.||||||02-FEB-05
37720|Marillana Formation|63432|5|Briefly described|p734, p736 Fig. 3|||Includes the Iowa Eastern, Barimunya and Munjina Members. Overlies Weeli Wolli Formation. Geological Province: Hamersley Province.||||||07-FEB-11
37720|Marillana Formation|65194|5|Briefly described|p107-111|||Comprises all fluvial sediments in Marillana Palaeovalley and tributaries, including the former Marillana Pisolite. Overlies Hamersley Group. Disconformably overlain by calcretised lacustrine carbonates and unconsolidated alluvium and colluvium. Includes Munjina, Barimunya and Iowa Eastern Members.||||||
37720|Marillana Formation|69538|5|Briefly described|p522 Fig.5, p532 Tb.3, p534-535|Miocene|Eocene|See also p557 Fig.32, p572, p583-585. Formerly the Robe Pisolite in the Yandi area. NE Hamersleys. Hosts the well-known Yandi CID CzD2 iron deposits, incised into Weeli Wolli Formation.|||Includes MunjinIncludes Munjina, Barimunya and Iowa Eastern Members.a and Barimunya Members.|||27-MAY-16
37720|Marillana Formation|72447|6|Mentioned|p237-238, p241|early Oligocene|late Eocene|Hamersley Region. Hosts fossiliferous iron-rich pisolitic deposits (channel iron deposits). Represents extensive pisolith deposits in the Marillana-Yandicoogina Creek area.||||||
37720|Marillana Formation|73574|5|Briefly described|p762|Miocene|Late Eocene|Central Hamersley region. See also Marillana Pisolite.|||Barimunya Member|||
79025|Marker Chert|65757|6|Mentioned|p83 Fig.3|||overlies the Kangaroo Caves Formation, [written as a formal name but probably intended as informal reference].||||||
79025|Marker Chert|69616|5|Briefly described|p159, p161-164, p167, p169, p171, p179|Archean|Archean|See also p184. Main host of the regionally-extensive Kangaroo Caves VHMS Zn-Cu mineralisation. Has three major alteration zones and distinct zonation of sulfides. 5-80m thick. Characterised by abundant folds and faults.||Topmost unit in Kangaroo Caves Formation.||Is overlain by Soanesville Group. Is intruded by neptunian sandstone dykes of Corboy Formation.|Chert.|
79025|Marker Chert|71808|5|Briefly described|p9|||Hamersley Province. Approximately 5m thick. Intersected in DDH186.|||||Mesobanded, planar bedded chert with minor interbedded black shales.|
28212|Marla Group|22901|6|Mentioned|76 fig 2|||Geol province Officer Basin||||||
28212|Marla Group|22922|5|Briefly described|34|||||||||
28212|Marla Group|23282|4|Described|p68||Neoproterozoic|Was 'Marla Sequence' of Krieg (1973) and defined as Marla Group by Benbow (1982).||||||24-SEP-08
28212|Marla Group|23288|6|Mentioned|Fig.5||Early Cambrian|||||||
28212|Marla Group|23479|5|Briefly described|p26|Paleozoic|Paleozoic|Geological Province: Gawler Craton [??more likely overlies].||||||04-NOV-10
28212|Marla Group|23557|5|Briefly described|p95 Fig.1|Neoproterozoic III|Neoproterozoic III|Geological Province: Officer Basin.||||||
28212|Marla Group|24112|5|Briefly described|p254 Fig.2|Middle Cambrian|Early Cambrian|Geological Province: Officer Basin||||||
28212|Marla Group|38329|2|Defined|p194|Cambrian|Cambrian|||||||
28212|Marla Group|40642|6|Mentioned|p175|||||||||
28212|Marla Group|40945|6|Mentioned|Fig.3|||||||||
28212|Marla Group|42065|5|Briefly described|p185|||See also Fig.2||||||
28212|Marla Group|42357|5|Briefly described|p10|||||||||
28212|Marla Group|43052|5|Briefly described|Fig.2.10|||||||||
28212|Marla Group|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Includes Wirrildar beds, Trainor Hill Sandstone, Mount Johns Conglomerate, Arcoeillinna Sandstone, Observatory Hill Formation and Wallatinna Formation.||||||
28212|Marla Group|43657|6|Mentioned|Fig.3,p4||Cambrian|||||||
28212|Marla Group|43690|6|Mentioned|Fig.2,p157||Cambrian|||||||
28212|Marla Group|43743|6|Mentioned|Fig.2,p33|Middle Cambrian|Early Cambrian|||||||
28212|Marla Group|44109|5|Briefly described|p22 Fig. 19|Cambrian|Cambrian|Includes the Relief Sandstone, Ouldburra, Observatory Hill and Wallatinna Formations, Arceollinna Sandstone, Mount Johns Conglomerate and Trainor Hill Sandstone. Geological Province: central Officer Basin.||||||
28212|Marla Group|44133|5|Briefly described|p35|||Includes the Refief Sandstone and the Ouldburra Formation.||||||
28212|Marla Group|60565|6|Mentioned|p18|Cambrian|Cambrian|||||||
28212|Marla Group|61732|5|Briefly described|p4 Fig. 3, p67-68|Cambrian|Marinoan|Includes the Relief Sandstone and Ouldburra and Observatory Hill Formations. Unconformably overlies Narana Formation and its Mena Mudstone member. Geological Province: eastern Officer Basin. See also p58 Fig. 22, p89.||||||17-APR-13
28212|Marla Group|62453|5|Briefly described|p5 Fig. 3|Cambrian|Cambrian|Geological Province: Officer Basin.||||||
28212|Marla Group|62570|5|Briefly described|p579, p580 Figs. 2 and 3|Middle Cambrian|Early Cambrian|Includes Relief Sst, Ouldburra and Observatory Hill Fm, Arcoeillinna and Trainor Hill Ssts. Thickness: >1.5km. Type section in Manya Trough area. Unconformable over Ungoolya Gp. Contains mainly siliciclastics with some carbonates. Geol.prov: Officer Basin||||||10-AUG-07
28212|Marla Group|63224|5|Briefly described|p8|Cambrian|Cambrian|Informally divided into upper and lower Marla Group on the basis of drillhole stratigraphy.||||||02-MAY-07
28212|Marla Group|64103|6|Mentioned|p400 Fig. 3|Cambrian|Cambrian|Geological Province: Officer Basin.||||||07-FEB-11
28212|Marla Group|64794|6|Mentioned|p240 Tb.1|Middle Cambrian|Early Cambrian|Officer Basin. 900m thick.||||||
28212|Marla Group|64970|6|Mentioned|p719 Fig. 2|Cambrian|Neoproterozoic|Geological Province: Officer Basin.||||||27-MAY-09
28212|Marla Group|65313|5|Briefly described|p578, Fig 6|Ordovician|Cambrian|Officer Basin. Ungoolya 1 well.|||Includes Observatory Hill Formation, Apamurra Formation, Trainor Hill Sandstone.|Underlies Munda Group.||26-MAR-12
28212|Marla Group|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Ediacaran|Eastern Officer Basin. Includes Ediacara fauna.||||||19-MAR-12
28212|Marla Group|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Ediacaran|Eastern Officer Basin. Includes Ediacara fauna||||||
28212|Marla Group|65376|5|Briefly described|p9 Fig.1.2. |Paleozoic|Paleozoic||||||Evaporitic fluvial, eolian and marine sediments.|
28212|Marla Group|67120|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Apamurra Formation, Arcoeillinna Sandstone, Observatory Hill Formation, Relief Sandstone, Trainor Hill Sandstone.||Sandstone, limestone, evaporites.|
28212|Marla Group|68131|5|Briefly described|p2 Fig.1|Cambrian|Cambrian|Evaporitic fluvial, aeolian and marine sediments.||||||
28212|Marla Group|69003|6|Mentioned|p60|Cambrian|Cambrian|E Officer Basin.||||||
28212|Marla Group|69648|4|Described|p19, p34-35, map legend|Middle Cambrian|Early Cambrian|Early to Middle Cambrian sediments of Tallaringa Trough (Relief Sandstone, Ouldburra Formation) may extend into northeastern OOLDEA.|Minimum: ~507 Ma||Relief Sandstone, Ouldburra Formation|||
28212|Marla Group|70336|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Trainor Hill, Relief, Arcoeillinna Sandstones; Apamurra, Observatory Hill Formations.||Sandstone, limestone, evaporites.|12-JAN-16
28212|Marla Group|71146|5|Briefly described|p6|Cambrian|Cambrian|Officer Basin.||||Overlain by the Table Hill Volcanics.|Sandstone, mudstone and evaporite.|
28212|Marla Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
28212|Marla Group|71268|5|Briefly described|1m_geologyp12_lut.csv||||||Includes Wirrildar beds.|||
28212|Marla Group|72476|5|Briefly described|p26, 35, p36 Fig.9|||Officer Basin. Sediments derived from the Musgrave Block. Early Paleozoic.|||||Clastic sedimentary rocks.|
28212|Marla Group|72478|5|Briefly described|p8, p9|Middle Cambrian|Early Cambrian|Officer Basin.|c. 545 Ma-510 Ma||Includes the Ouldburra Formation, Relief Sandstone, Observatory Hill Formation, Arcoeillinna Sandstone, Apamurra Formation, Trainor Hill Sandstone.|||25-MAR-21
28212|Marla Group|73090|5|Briefly described|p12 Fig.7|Cambrian|Cambrian||||Observatory Hill Formation, Trainor Hill Sandstone.|||
28212|Marla Group|73099|5|Briefly described|Map legend.|Middle Cambrian|Early Cambrian|Officer Basin.|||Relief, Arcoeillinna, Trainor Hill Sandstones; Observatory Hill, Apamurra Formations.|Overlies Ungoolya Group. Is overlain by Munda Group.||
74955|Marlomumbah Granite|64891|5|Briefly described|p37 Fig. 2, p52-53 Tb. 1|Archean|Archean|Of Wogala Suite (Bald Rock Supersuite). Age: c. 2625Ma. Geological province: Murchison Domain. Fluorite-bearing alkali granite; post-tectonic.||||||07-FEB-11
74955|Marlomumbah Granite|65548|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Wogala Suite, Bald Rock Supersuite, Yilgarn Craton. Muscovite-bearing alkali granite; equiganular; contains accessory fluorite; post-tectonic.||||||
74955|Marlomumbah Granite|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. U-Pb zircon age: 2606 +/- 5 Ma for the 13 analyses is interpreted as the magmatic crystallization age of the granodiorite. See geochron file 185929.1.pdf.||Wogala Suite||Pegmatites from this granite crosscut a Cullculli Suite tonalite and probably Jungar and Walganna Suites too (aeromag data).|Muscovite-bearing alkali granite; equigranular; common accessory fluorite|23-OCT-15
74955|Marlomumbah Granite|69583|5|Briefly described|p49; Plate 2|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Wogala Suite.|||Muscovite-bearing alkali granite; common accessory fluorite.|
74955|Marlomumbah Granite|69584|5|Briefly described|p5 Fig.2|Neoarchean|Neoarchean|||Wogala Suite|||Granite.|
74955|Marlomumbah Granite|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Wogala Suite.||||
74955|Marlomumbah Granite|70796|5|Briefly described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton. See also 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 185929.1.pdf, Madoonga100_2444_stratig.pdf.|2606 +/ 5 Ma (isotopic)|Wogala Suite||Intrudes the Cullculli Suite and the Jungar and Walganna suites.|Muscovitebearing alkali granite; equigranular; common accessory fluorite.|
74955|Marlomumbah Granite|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma). Sample GSWA 185929 (granodiorite) yielded a concordia age of 2606 +\-5 Ma, interpreted as the magmatic crystallization age of the granodiorite. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv.|2626+\-5 Ma|Unit of Wogala Suite.||In contact with, and intrudes into Culculli Suite tonalites.|Muscovite-bearing alkali granite; equigranular; common accessory fluorite|
74955|Marlomumbah Granite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||2606+/-5 Ma.|Wogala Suite|||Muscovite-bearing alkali granite; equigranular; common accessory fluorite.|
80594|Marnda Moorn Suite|66106|6|Mentioned|p45|||Appears as Marnda Moorn Dolerite Suite.|1200 Ma.|||||
80594|Marnda Moorn Suite|72389|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Marnda Moorn Large Igneous Province. Gabanintha 1:100k map sheet 2644.|||Includes the Muggamurra Dolerite.|||28-AUG-20
80594|Marnda Moorn Suite|73410|6|Mentioned|p12|||Murchison Domain, Yilgarn Craton.|c.1210 Ma.|||||
26017|Marradong Formation|33800|2|Defined|p138|Archean|Archean|Type area on Mount Saddleback, where the most continuous section is, in a 400m long eye-shaped incision into the laterite surface, 2 km south of Marradong. 3-8 km of metabasalt with apparently only minor intercalations of dark metasediment and rare metadacite.||||Conformably overlies Wells Formation.||14-FEB-18
26017|Marradong Formation|37017|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
26017|Marradong Formation|40359|6|Mentioned|p9|||||||||
26017|Marradong Formation|40360|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
26017|Marradong Formation|40370|6|Mentioned|p37|||||||||
26017|Marradong Formation|40775|4|Described|p494|||||||||
26017|Marradong Formation|40785|6|Mentioned|Fig.1|||||||||
26017|Marradong Formation|41066|6|Mentioned|2 of 2 C05|||||||||
26017|Marradong Formation|41378|6|Mentioned|p77|||||||||
26017|Marradong Formation|42165|5|Briefly described|p92|||||||||
26017|Marradong Formation|43061|6|Mentioned|p31|||||||||
26017|Marradong Formation|64016|6|Mentioned|p12, p12 Fig. 4|||Mafic volcanic rocks.||||||
67831|Marron Member|6943|4|Described|p599, p601, p603, p605, pp607-608.|Early Silurian|Late Ordovician|Siltstones produce high gamma ray logs. Oxidisation implies exposure to weathering; probably post-Carboniferous to at least Early Cretaceous before being reburied.||Unit in Ajana Formation.||Is disconformably overlain by Coburn Formation in BHP ND 002.|Lithologically distinctive siliciclastic unit, mainly pale grey, oxidised siltstone with medium-grained sandstone; local thin gypsum and dolomite beds.|
67831|Marron Member|12729|4|Described|Figs. 8, 9, 23; p. 5, 8, 10, 30, 32|Early Silurian|Late Ordovician|Named after Marron Station (Mory et al. 1998b). Type section: fully cored 912-974 m interval in Coburn 1. A general Late Ordovician to Early Silurian age indicated (Backhouse, 1999). Thickens NW (53 m in Kalbarri 1, 148 m in Dirk Hartog 17B).||Ajana Formation (Dirk Hartog Group)||Overlies the Tumblagooda Sandstone. Is disconformably overlain by Coburn Formation.|Pale-grey, largely oxidized siltstone with medium-grained sandstone capping the basal shoaling-up cycle, often capped by a dolomitic section. Locally contains thin gypsum and dolomite beds.|17-SEP-15
67831|Marron Member|14228|5|Briefly described|p4, p6 fig3, p18|Llandovery|Ashgill|May be genetically related to the underlying redbed facies, rather than the shallow-marine carbonate and mud facies of Ajana Formation. Shale to 100m thick; may seal Tumblagooda Sandstone.||At base of Ajana Formation (Dirk Hartog Group).||Overlain in part (disconformably) by Coburn Formation.|Oxidized siltstone.|
67831|Marron Member|23572|6|Mentioned|p10|||Geological Province: Carnarvon Basin.||||||
67831|Marron Member|23935|5|Briefly described|p19|||Basal part of the Ajana Formation. Geological Province: Southern Carnarvon Basin.||||||27-JAN-05
67831|Marron Member|50084|5|Briefly described|p77 Fig.2|Ordovician|Ordovician|Of Ajana Formation. Brown to grey mudstone with fine-grained sandstone. Thickness: 65 m. Geological Province: Southern Carnarvon Basin.||||||07-FEB-11
67831|Marron Member|65313|5|Briefly described|p578|Llandovery|Llandovery|In Coburn 1 well. Contains Telychian (latest Llandovery) conodonts.||Of Ajana Formation, in Coburn 1 well.||Overlies Tumblagooda Sandstone.||26-MAR-12
67831|Marron Member|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.||Ajana Formation|||Includes dark blue/grey claystone; pale tan claystone with numerous grey salt patches.|
67831|Marron Member|67200|6|Mentioned|p18 table 1, p46, p52, p56, app 2 p4|||Thermal conductivity of 2.09 W/mK||Ajana Formation|||Claystone with numerous salt patches.|
79020|Marshall Pool Subgroup|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2720 - 2680 Ma (inferred).||Mount Fouracre Basalt, Mount Clifford Komatiite, Hangover Formation.||Basalt, komatiitic basalt, komatiite, mafic schist, metamorphosed sandstone and siltstone, felsic volcaniclastic and volcanic rocks.|
79020|Marshall Pool Subgroup|71270|5|Briefly described|100k_interpgeop_lut.csv|||Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Metamorphosed to greenschist facies. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma). Tectonically juxtaposed against Gindalbie Group along the Ockerburry and Perseverance Faults. Sample GSWA 211056 (metarhyolite) yielded a weighted mean 207Pb/206Pb date of 2736+\-6 Ma, interpreted as the magmatic crystallization age of the rhyolite.||Unit of Kalgoorlie Group.|Includes Hangover Formation, Mount Clifford Komatiite, Mount Fouracre Basalt.|Underlain by Mount Leonora Formation.|Mafic and ultramafic rocks with minor sedimentary and felsic volcanic rocks.|
79020|Marshall Pool Subgroup|72095|6|Mentioned|p5 Fig 3|Neoarchean|Neoarchean|Eastern Goldfields, Yilgarn Craton.||Unit of Kalgoorlie Group.||||
79020|Marshall Pool Subgroup|73596|5|Briefly described|p1159, 1163-1165|Neoarchean|Neoarchean|Leonora eastern domain, Kalgoorlie Terrane.|2736 +/- 10 Ma (Pidgeon and Wilde, 1990).||Hangover, Mount Fouracre Basalts; Mount Clifford Komatiite.|Paraconformably overlies Mount Leonora Formation. Is overlain by Gindalbie Group.|Mafic and ultramafic volcanic rocks.|
37104|Marty Bore Granite|23751|6|Mentioned|p11|||||||||
78755|Mary Bore Granite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2760 - 2600 Ma (inferred).||||Quartz-feldspar-biotite granite; massive to foliated.|
78755|Mary Bore Granite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). Type area: MENZIES (SH 51-5), MELITA (3139); pavement outcrop 6.2km S of Six Mile Well, 5.5 km WNW of Charcoal Well, and 1.0 km NE of Mary Bore. Sample GSWA 211059 (metamonzogranite) yielded a weighted mean 207Pb/206Pb date of 2664+\-3 Ma, interpreted as the magmatic crystallization age of the monzogranite.|2760-2640 Ma (inferred)||||Quartz-feldspar-biotite granite; massive to foliated; metamorphosed|
67998|Mason Conglomerate|62453|3|Fully described|p5 Fig. 3, 10, 40, 42|Cryogenian|Cryogenian|Of the Buldya Group. Geological Province: Officer Basin. Overlies: Ilma Formation.||||||
67998|Mason Conglomerate|62987|5|Briefly described|p30|||Probably of the Buldya Group? Geological Province: Officer Basin.||||||
67998|Mason Conglomerate|64103|5|Briefly described|p400 Fig. 3|Cryogenian|Cryogenian|Conglomerate is Cgl in text. Geological Province: Officer Basin.||||||07-FEB-11
67998|Mason Conglomerate|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|Officer Basin.||Buldya Group.||||
75242|Mason Knob Monzogranite|66116|5|Briefly described|Map legend|Archean|Archean|Yilgarn Craton. 2660 +/- 3 Ma. Metamorphosed porphyritic monzogranite; fine- to coarse-grained with feldspar megacrysts; locally seriate.||||||
75242|Mason Knob Monzogranite|69152|5|Briefly described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Porphyritic monzogranite; fine- to coarse-grained with feldspar megacrysts, locally seriate; metamorphosed.|06-AUG-15
75242|Mason Knob Monzogranite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|See also 100k_geologyp14_lut.csv and 500k_interpgeop14_lut.csv.|2660 +/- 3 Ma (isotopic).||||Porphyritic monzogranite; fine- to coarse-grained with feldspar megacrysts, locally seriate; metamorphosed.|
75242|Mason Knob Monzogranite|70802|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism.|2660+\-3 Ma||||Porphyritic monzogranite; fine- to coarse-grained with feldspar megacrysts, locally seriate; metamorphosed|
75242|Mason Knob Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 100k_geologyp14_lut.csv, 500k_interpgeop_lut.csv, 2_5m_interpgeop15_lut.csv.|2660+\-3 Ma||||Porphyritic monzogranite; fine- to coarse-grained with feldspar megacrysts, locally seriate; metamorphosed|
75242|Mason Knob Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||2660+/-3 Ma.||||Porphyritic monzogranite; fine- to coarse-grained with feldspar megacrysts, locally seriate; metamorphosed.|
36102|Matchbox Granite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1850Ma. Geological province: Kimberley Province (East).||||||07-FEB-11
36102|Matchbox Granite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
36102|Matchbox Granite|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite.||||||07-NOV-08
36102|Matchbox Granite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Paperbark Supersuite.|||Medium- and coarse-grained porphyritic biotite monzogranite and syenogranite|
36102|Matchbox Granite|72437|5|Briefly described|p89|||Lamboo Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Porphyritic biotite monzogranite.|
31884|Maude Headley Member|22496|5|Briefly described|p7|Paleoproterozoic|Paleoproterozoic|Of the Olympio Formation (Halls Creek Group).  Age: 1857+/-2Ma.||||||07-NOV-08
31884|Maude Headley Member|22526|5|Briefly described|P680, Fig3 P682||Orosirian|||||||
31884|Maude Headley Member|22754|4|Described|p3|Paleoproterozoic|Paleoproterozoic|Of the Olympio Formation.  Age: 1857+/-5Ma (SHRIMP).||||||07-NOV-08
31884|Maude Headley Member|23383|5|Briefly described|p12|Paleoproterozoic|Paleoproterozoic|Of Olympio Formation.  Age: 1857+/-5 Ma (SHRIMP U-Pb zircon).||||||07-NOV-08
31884|Maude Headley Member|23599|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic|Of Olympio Formation. Geological Province: Lamboo Complex.||||||07-NOV-08
31884|Maude Headley Member|23621|2|Defined|p54 Appendix|Orosirian|Orosirian|See also page 16, 11 table 1. Age: ~1857 Ma. Of Olympio Formation. Overlying unit Butchers Gully Member. Underlying unit Biscay Formation. Halls Creek Orogen. Max. thickness: >1000 m.||||||
31884|Maude Headley Member|23622|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Halls Creek Group.||||||07-NOV-08
31884|Maude Headley Member|24173|3|Fully described|p17, p13 Tb.2|Paleoproterozoic|Paleoproterozoic|Of the Olympio Fm. Geological Province: Halls Creek Orogen. Max Thickness: >1000m. An extrusive flow previously mapped within the Biscay Fm (now referred to as the "Biscay Formation rhyolite sill") is included within this member. Age: 1857Ma. See also p16||||||07-NOV-08
31884|Maude Headley Member|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Olympio Formation (Halls Creek Group).  Metamorphosed andesitic to trachytic volcanic and volcaniclastic rocks with carbonate-rich matrix, ferruginous chert, mudstone and turbiditic wacke.||||||07-NOV-08
31884|Maude Headley Member|24572|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Olympio Formation.  Age: >1835Ma.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
31884|Maude Headley Member|43854|5|Briefly described|Map Legend||Proterozoic|of Olympio Formation.||||||
31884|Maude Headley Member|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31884|Maude Headley Member|50437|5|Briefly described|p1.7, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Butchers Gully Suite.||||||07-NOV-08
31884|Maude Headley Member|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Olympio Formation (Halls Creek Group). Age: c. 1855Ma. Metamorphosed andesitic to trachytic volcanic and volcaniclastic rock with carbonate-rich matrix; minor ferruginous chert.||||||
31884|Maude Headley Member|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Of Olympio Formation. Metamorphosed andesitic to trachytic volcanic and volcaniclastic rocks with carbonate-rich matrix, ferruginous chert, and mudstone and turbiditic greywacke.||||||15-DEC-08
31884|Maude Headley Member|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Felsic extrusive dated for crystallisation age. Data published in 2000.|1847+/-6 Ma, 1857+/-5 Ma U/Pb SHRIMP|Olympio Formation|Includes 2 unnamed subunits.||Meta-andesitic to metatrachytic volcanic and volcaniclastic rocks with carbonate-rich matrix, ferruginous metachert, and metamudstone and turbiditic metasandstone; metamorphosed felsic sill; metatrachyte lava flows and domes.|03-AUG-15
31884|Maude Headley Member|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv. |1856-2460 Ma||||Meta-andesitic to metatrachytic volcanic and volcaniclastic rocks with carbonate rich matrix, ferruginous metachert, and metamudstone and turbiditic metasandstone. Metatrachyte lava flows and domes, metamorphosed felsic sill.|
31884|Maude Headley Member|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|1857-1857 Ma (Isotopic)|Unit of Olympio Formation.|||Meta-andesitic to metatrachytic volcanic and volcaniclastic rocks (lava and domes) with carbonate-rich matrix, ferruginous metachert, and metamudstone and turbiditic metasandstone, metamorphosed felsic sills|
31884|Maude Headley Member|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv.|1857 Ma||||Meta andesitic to metatrachytic volcanic and volcaniclastic rocks with carbonate rich matrix, ferruginous metachert, metamudstone and turbiditic metasandstone.|
31884|Maude Headley Member|71113|5|Briefly described|p96-97|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen. Zircon age dating of 1857+\-5 Ma (Page and Hancock, 1988).||Unit of Olympio Formation.||Lower unit of Olympio Formation. Underlain disconformably by Biscay Formation.|Trachyandesitic and trachytic rocks.|
31884|Maude Headley Member|71140|6|Mentioned|p96-97|Orosirian|Orosirian|Eastern Zone, Lamboo Province, Halls Creek Orogen.|1857 +/- 5 Ma (Page and Hancock, 1988).|Olympio Formation.||||
31884|Maude Headley Member|71267|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See also geochron files.|1856+\-6 Ma (isotopic)|Unit of Olympio Formation.|||Meta-andesitic to metatrachytic volcanic and volcaniclastic rocks (lava flows and domes) with carbonate-rich matrix, ferruginous metachert, and metamudstone and turbiditic metasandstone|
31884|Maude Headley Member|71397|4|Described|p4-5,7,16,18,32, 38-39,41,44-46,48|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen. Crops out in a series of NNE trending outcrops 5 km NE of Sophie Downs Dome and Saunders Creek Dome.  Discrete volcanic centre of submarine alkaline lavas and associated volcaniclastic unit punctuating deep-marine sedimentation. Occurs 50-100m stratigraphically above the base of Olympio Formation. Base of the member is identified by presence of 0.5-1.5m thick breccia beds. Zircon U-Pb geochronological analysis of sample GA 85598001 (felsic volcanic rock) yielded a weighted mean 207Pb*/206Pb* date of 1856+\-6 Ma, interpreted as age of volcanism.|1856+\-5 Ma|Unit of Olympio Formation.|||Metamorphosed alkali volcanic and volcaniclastic rocks with a carbonate matrix and breccia beds.|28-NOV-19
31884|Maude Headley Member|71873|6|Mentioned|p426,443|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province.||||||
23772|Maudoobar Sandstone|13194|4|Described|p392 Tb. 4-16, p402 fig 4-66|Frasnian|Frasnian|Type Section: near Cockatoo Spring 15o53'S 128o58'E. 320-400 unfossiliferous quartz sandstone (eolian).||Cockatoo Group||Conformable within Cecil Sandstone.|Quartz sandstone.|
23772|Maudoobar Sandstone|40993|2|Defined|p6|Frasnian|Frasnian|||||||
23772|Maudoobar Sandstone|41864|3|Fully described|p54|||Probably lens within Cecil Sandstone (see p54)||||||
23772|Maudoobar Sandstone|41865|5|Briefly described|Map legend|Frasnian||||||||
23772|Maudoobar Sandstone|42030|5|Briefly described|p749|||||||||
23772|Maudoobar Sandstone|69452|6|Mentioned|p36:6|Frasnian|Frasnian|||Cockatoo Group.||||12-JUL-16
42116|Maverick Monzogranite|23809|5|Briefly described|p16|Paleoproterozoic|Paleoproterozoic|Equigranular, homogeneous, undeformed hornblende-biotite monzogranite to granodiorite.||||||07-NOV-08
42116|Maverick Monzogranite|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1801+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Monzogranite.|
23773|May River Conglomerate|40793|6|Mentioned|p164|||||||||
23773|May River Conglomerate|40837|6|Mentioned|p260|||||||||
23773|May River Conglomerate|43563|6|Mentioned|p17|||||||||
36844|Maydon Basalt|23727|4|Described|p9|||Overlying unit Hatfield Formation. Underlying unit Bandalup Ultramafics. Geological Province: Carlingup Terrane. Max. thickness: 2000 m.||||||
36844|Maydon Basalt|23728|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Hatfield Formation. Underlying unit Bandalup Ultramafics. Geological Province: Yilgarn Craton.||||||07-NOV-08
36844|Maydon Basalt|23752|4|Described|p6|Archean|Archean|Geological Province: Carlingup Terrane.||||||07-NOV-08
36844|Maydon Basalt|23754|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Hatfield Formation. Underlying unit Bandalup Ultramafics. Geological Province: Yilgarn Craton.||||||07-NOV-08
36844|Maydon Basalt|64580|4|Described|map legend|Neoarchean|Mesoarchean|Metabasalt, commonly pillowed with minor interflow sedimentary rocks; dolerite; amphibolite.||||||15-DEC-08
36844|Maydon Basalt|65487|6|Mentioned|p6|||Overlies the Bandalup Ultramafics and underlies the Hatfield Formation in the Carlingup Greenstone Belt; consists of pillowed metabasalt with minor metadolerite and rare interflow metasediments; the basalt is siliceous and high-Mg. 2 km thick.||||||
36844|Maydon Basalt|69404|5|Briefly described|p10, p10 Fig.11|||Carlingup Terrane.||||Overlies the Bandalup Ultramafics, overlain by the Hatfield Formation.|Massive to pillowed basalt; commonly variolitic; locally with pyroxene-spinifex texture, minor dolerite.|
36844|Maydon Basalt|69559|5|Briefly described|500k_geologyp08_lut.csv|Neoarchean|Mesoarchean||||||Metabasalt, commonly pillowed with minor interflow sedimentary rocks; dolerite; amphibolite.|
36844|Maydon Basalt|69617|6|Mentioned|p155|||||||Is overlain by Hatfield Formation.||
36844|Maydon Basalt|70156|4|Described|500k_interpgeop14_lut.csv|Mesoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma).|3200-2958 Ma (inferred)||||Metabasalt, commonly pillowed with minor interflow sedimentary rocks; minor dolerite and amphibolite|
36844|Maydon Basalt|70794|4|Described|500k_interpgeop14_lut.csv|Mesoarchean|Mesoarchean|Youanmi Terrane, Yilgarn Craton. Also 2_5m_interpgeop15_lut.csv, where age range given as 3131-2958 Ma inferred.|3200-2958 Ma inferred.||||Metabasalt, commonly pillowed with minor interflow sedimentary rocks; minor dolerite and amphibolite.|
36844|Maydon Basalt|70802|5|Briefly described|500k_interpgeop14_lut.csv|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Youanmi Terrane events.|3200-2958 Ma (inferred)||||Metabasalt, commonly pillowed with minor interflow sedimentary rocks; minor dolerite and amphibolite|
36844|Maydon Basalt|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Youanmi Terrane.|||||Metabasalt, commonly pillowed with minor interflow sedimentary rocks; minor dolerite and amphibolite.|
29542|McAuliffe Well Syenite|23786|5|Briefly described|p35 Tb. 4|||Geological Province: Yilgarn Craton.||||||
29542|McAuliffe Well Syenite|24196|5|Briefly described|p44|Archean|Archean|Age: 2651 +/- 5 Ma (Nelson, 1997a)||||||07-NOV-08
29542|McAuliffe Well Syenite|24494|5|Briefly described|p21, p38 App.1|Archean|Archean|Age: 2651 +/- 5 Ma (U-Pb zircon; Nelson, 1997a)||||||07-NOV-08
29542|McAuliffe Well Syenite|44203|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
29542|McAuliffe Well Syenite|64775|6|Mentioned|p4-1|Neoarchean|Neoarchean||2651+/- 5 Ma.|||||30-MAR-12
29542|McAuliffe Well Syenite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Medium- to coarse-grained quartz syenite; K-feldspar megacrysts.||||||07-FEB-11
29542|McAuliffe Well Syenite|69152|5|Briefly described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Medium- to coarse-grained quartz syenite; K-feldspar megacrysts.|06-AUG-15
29542|McAuliffe Well Syenite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Medium- to coarse-grained quartz syenite; K-feldspar megacrysts.|
29542|McAuliffe Well Syenite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||syenite|
29542|McAuliffe Well Syenite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. See 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|||||Medium- to coarse-grained quartz syenite; K-feldspar megacrysts|
28737|McHale Granite|36551|6|Mentioned|p48|||||||||
28737|McHale Granite|44317|5|Briefly described|Table 1||Proterozoic|||||||
28737|McHale Granite|44318|14|Not recorded|map legend||Proterozoic|Proterozoic.||||||
28737|McHale Granite|45047|6|Mentioned|p72|||||||||
28737|McHale Granite|60533|5|Briefly described|p604|Paleoproterozoic|Paleoproterozoic|Age: 1827 +/- 3Ma. Geological Province: Halls Creek Orogen. Overlain unconformably by Red Rock Formation.||||||07-NOV-08
28737|McHale Granite|66845|4|Described|p539 Tb.1, p542|||Complex, euhedral zircon population. Analysed cores represent source-rock inheritance or crustal contamination. Discordant data rejected, remaining 20 data points 207Pb/206Pb cluster represents best interpreted magmatic age so far for this unit.|interpreted magmatic age, 1827+/-3 Ma SHRIMP U-Pb||||biotite monzogranite|
28737|McHale Granite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Mabel Downs Suite|||Medium-coarse grained equigranular biotite-hornblende tonalite and biotite granodiorite; extensive magmatic brecciation and associated alteration.|
78624|McIntosh Suite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. K/Ar ages: 1729, 1732 from McIntosh Gabbro in Bofinger, V.M. 1967. Geochronology in the east Kimberley area of Western Australia. SHRIMP Data from OZCHRON1. Comment: (1855 Ma)'This zircon crystallisation age for the group III Toby mafic intrusion is based on 24 concordant data points, and is indistinguishable from the age of the Panton and Springvale intrusions.' (1842 Ma) 'This is the zircon U-Pb age for igneous crystallisation of the Sally Malay mafic-ultramafic intrusion (group IV). It is in good agreement with 30 baddelyite analyses from the same rock (weighted mean 1846+/-5 Ma)|SHRIMP 1855+/-2 Ma, 1842+/-3 Ma.|Sally Downs Supersuite|Includes 4 unnamed units.||Layered mafic-ultramafic intrusions: magnetite gabbro, magnetite gabbronorite, magnetite-olivine gabbro, olivine gabbro, leucogabbro, leucogabbronorite, anorthosite, olivine gabbronorite, gabbro, gabbronorite, peridotite and troctolite|03-AUG-15
78624|McIntosh Suite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Sally Downs Supersuite|||Magnetite gabbro, magnetite gabbronorite, magnetite-olivine gabbro, olivine gabbro, leucogabbro, leucogabbronorite, anorthosite,peridotite and minor troctolite.|
78624|McIntosh Suite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2.|1830-1808 Ma (Isotopic)||||Layered mafic-ultramafic intrusions; magnetite gabbro, magnetite gabbronorite, magnetite-olivine gabbro, olivine gabbro, leucogabbro, leucogabbronorite, anorthosite, and minor troctolite, peridotite, troctolite|
78624|McIntosh Suite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1808-1830 Ma|Sally Downs Supersuite|||Layered mafic and ultramafic intrusions, magnetite gabbro, magnetite gabbronorite, magnetite-olivine gabbro, olivine gabbro, leucogabbro, leucogabbronorite, anorthosite and minor troctolite.|
78624|McIntosh Suite|70812|4|Described|p6, p8-p9, p43|Orosirian|Orosirian|Central Zone of the Halls Creek Orogen, Lamboo Province.|c. 1830 Ma|||Intrudes the Tickalara Metamorphics.|Olivine gabbro and gabbronorite, troctolite, mangetite gabbro, leucogabbro and peridotite.|
78624|McIntosh Suite|70851|5|Briefly described|p4, p24|Paleoproterozoic|Paleoproterozoic|Lamboo Province. Emplaced at 18km depth. Geophysical characteristics are discussed.|c. 1830 Ma||||Mafic magmatics.|
78624|McIntosh Suite|71113|5|Briefly described|p99|Orosirian|Orosirian|Geological province: Central Zone, Lamboo Province, Halls Creek Orogen. Part of a suite of large gabbroic and layered mafic-ultramafic bodies intruding into the Central Zone.|c. 1830 Ma|||||
78624|McIntosh Suite|71140|6|Mentioned|p99|Orosirian|Orosirian|Central Zone, Lamboo Province, Halls Creek Orogen.|c.1830 Ma.||||Large gabbroic and layered mafic-ultramafic bodies.|
78624|McIntosh Suite|71267|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma).|1830+\-3 to 1808 Ma (isotopic, inferred)|Unit of Sally Downs Supersuite.|||Leucogabbro, leucogabbronorite, anorthosite, and minor troctolite; magnetite gabbro, magnetite gabbronorite, magnetite-olivine gabbro, olivine gabbro, peridotite.|
31794|McIntosh intrusion|43854|5|Briefly described|Map Legend||Proterozoic|Variation on McIntosh Gabbro?||||||
31794|McIntosh intrusion|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31794|McIntosh intrusion|60498|5|Briefly described|p1016 Fig.1, p1017, pp1019-1020.|Paleoproterozoic|Paleoproterozoic|No lithology was stated for the stratigraphic name, except for the caption referring to 'mafic-ultramafic intrusions'. Halls Creek Orogen. The correct name is McIntosh Gabbro. Intrusions form dipping sheets, basins, large funnels, faulted blocks. Cu, Ti, V mineralisation. Electron microprobe geochemical analyses of apatites are detailed.|1830 +/- 3 Ma (Page & Hoatson 2000).||||Layered mafic-ultramafic intrusion: olivine gabbro and gabbronorite, gabbro, troctolite, magnetite gabbro, anorthositic gabbro, lherzolite.|03-JAN-18
31794|McIntosh intrusion|63866|5|Briefly described|p131, p138|Orosirian|Orosirian|Central Zone, Halls Creek Orogen. Numeric age is the dating of migmatisation in the contact aureole around this intrusion and is interpreted to closely approximate the emplacement age of this unit.|c. 1830 Ma (Page and Hoatson)|||||
31794|McIntosh intrusion|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Layered mafic-ultramafic intrusions; peridotite, troctolite, gabbro, olivine gabbro, gabbronorite, magnetite gabbro, magnetite-olivine gabbro, leucogabbro, leucogabbronorite, and anorthosite.||||||
31794|McIntosh intrusion|69099|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|Replaced by McIntosh Gabbro, McIntosh Suite? Grouped as McIntosh, Armanda, and Spring Creek intrusions, with single lith description in 500k_geologyp08_lut.csv. |||||Layered mafic-ultramafic intrusions; peridotite, troctolite, gabbro, olivine gabbro, gabbronorite, magnetite gabbro, magnetite-olivine gabbro, leucogabbro, leucogabbronorite, and anorthosite.|03-AUG-15
31794|McIntosh intrusion|69585|5|Briefly described|p31|Orosirian|Orosirian|Central Lamboo Province. 7.8km thick. Geochemistry indicates mantle sources modified by subduction processes.|c.1830 Ma.||||Large layered mafic intrusion.|
31794|McIntosh intrusion|71113|6|Mentioned|p96|||Geological province: Central Zone, Lamboo Province, Halls Creek Orogen. See McIntosh Suite.||||||
76190|McKay Creek Metasyenogranite|68186|5|Briefly described|p19, p79-81, Plates 1A, 2|Paleoproterozoic|Paleoproterozoic|One of the oldest dated intrusive rocks in the Biranup Zone, Kepa Kurl Booya Province. Forms bouldery hills c.15m high.|1761 +/- 10 Ma (GSWA 182424).|||Intruded by Bobbie Point Metasyenogranite.|Medium-grained, equigranular, K-feldspar-rich metasyenogranite. Undeformed to moderate NE-trending foliation. Mingling of this alkaline granitic magma with metagabbro and quartz metadiorite has produced dioritic hybrid rocks.|
76190|McKay Creek Metasyenogranite|69595|5|Briefly described|p6|Statherian|Statherian|Magmatic crystallization age.Maximum age from GSWA 182424. Eastern Biranup Zone. |1761 +/- 10 Ma  - 1650 Ma (Spaggiari et al. 2011)||||Metasyenogranitic rocks.|
76190|McKay Creek Metasyenogranite|70089|6|Mentioned|p263|Paleoproterozoic|Paleoproterozoic|Tropicana Zone, NE Albany-Fraser Orogen.||||||
76190|McKay Creek Metasyenogranite|70182|6|Mentioned|p4|||Tropicana Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen. Said to be "associated with" the Voodoo Child Formation.|c.1763 Ma.|||||
76190|McKay Creek Metasyenogranite|70256|5|Briefly described|p4, p24, p28|Paleoproterozoic|Paleoproterozoic|Kirkland et al. (2012). Tropicana Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen. Emplaced during the c.1770 Ma Ngadju Event.|c.1763 Ma.|||||
76190|McKay Creek Metasyenogranite|70802|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Geological province: Biranup Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen, West Australian Craton. Occurs in the far NE part of the Albany-Fraser Orogen, and is regularly exposed along McKay Creek. Sample GSWA 182424 yielded a concordia age of 1761+\-10 Ma, interpreted as the magmatic crystallization age of the syenogranite. Events: Albany-Fraser Orogeny Stage II (1225-1140 Ma); Albany-Fraser Orogeny (1330-1140 Ma); Albany-Fraser Orogeny Stage I (1330-1260 Ma); Biranup Orogeny (1710-1620 Ma); Ngadju Event (1780-1760 Ma). See 500k_interpgeop14_lut.csv, 250k_pre_mesozoic_interpgeop_lut.csv.|1761+\-10 Ma||||Metasyenogranite, mingled with metagabbro; may include intrusions of Bobbie Point Metasyenogranite, and remnants of Voodoo Child Formation and Tropicana Gneiss|
76190|McKay Creek Metasyenogranite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Tropicana Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen.|1761+/-10 Ma|||May include intrusions of Bobbie Point Metasyenogranite, and remnants of Voodoo Child Formation and Hercules or Tropicana Gneiss.|Metasyenogranite, mingled with metagabbro; may include intrusions of Bobbie Point Metasyenogranite, and remnants of Voodoo Child Formation and Hercules or Tropicana Gneiss.|
26023|McPhee Formation|23416|5|Briefly described|Map Legend|Archean|Archean|Of Talga Talga Subgroup. Geological Province: Pilbara Craton.||||||11-APR-13
26023|McPhee Formation|23755|4|Described|p19|Archean|Archean|See also page 17 table 1. Of Warrawoona Group. Max. thickness: 3000 m.||||||11-APR-13
26023|McPhee Formation|23783|4|Described|p12 Tb. 1|Archean|Archean|Of Talga Talga Subgroup.  See also p98.||||||07-NOV-08
26023|McPhee Formation|23807|6|Mentioned|p110 Fig. 2|||Geological Province: Pilbara Craton.||||||
26023|McPhee Formation|24025|4|Described|p9 Tb. 1|Archean|Archean|Of Talga Talga Subgroup. Talc-chlorite schist and talc-carbonate schist, chert, banded iron formation, basalt, pelite.  Max. Thickness: 200m.  Geological Province: Pilbara Craton.||||||07-NOV-08
26023|McPhee Formation|24184|5|Briefly described|p701, p699 Fig.4, p708|Archean|Archean|Of the Talga Talga Subgroup. Underlain by North Star Basalt. Geological Province: Pilbara Craton. Age: ca. 3477Ma||||||07-NOV-08
26023|McPhee Formation|24531|5|Briefly described|p5 Tb. 1|Archean|Archean|Of the Talga Talga Subgroup (Warrawoona Group). Geological Province: Pilbara Craton.||||||07-NOV-08
26023|McPhee Formation|24550|5|Briefly described|p31 Tb. 3.1|Archean|Archean|Of the Talga Talga Subgroup (Warrawoona Group). Felsic schist. The basal Big Chert unit of this formation overlies the North Star Basalt. Age: 3477Ma. Thickness: 500m. Geological Province: Pilbara Craton. See also p67.||||||07-FEB-11
26023|McPhee Formation|24590|5|Briefly described|p29, p30 Fig. 1.3|Archean|Archean|Of the Talga Talga Subgroup (Warrawoona Group). Talc chlorite schist, chert, BIF, pelite. Overlies the North Star Basalt; underlies Mount Ada Basalt. Age: 3477+/-2Ma (Nelson 2000). Thickness: 50-200m.||||||07-FEB-11
26023|McPhee Formation|31309|2|Defined|p53|Archean|Archean|||||||07-NOV-08
26023|McPhee Formation|38498|4|Described|p60|||See also Table 1.||||||
26023|McPhee Formation|38510|6|Mentioned|Fig.1|||||||||
26023|McPhee Formation|38544|6|Mentioned|Fig.1|||||||||
26023|McPhee Formation|39672|6|Mentioned|Fig.2|||||||||
26023|McPhee Formation|39697|3|Fully described|p89|||||||||
26023|McPhee Formation|40596|6|Mentioned|Fig.1|||||||||
26023|McPhee Formation|41029|5|Briefly described|p106|||||||||
26023|McPhee Formation|41624|6|Mentioned|p44|||See also P45||||||
26023|McPhee Formation|43595|6|Mentioned|Table 2-28,p214|||||||||
26023|McPhee Formation|43698|6|Mentioned|p26|||||||||
26023|McPhee Formation|43769|6|Mentioned|p858|||||||||
26023|McPhee Formation|44150|5|Briefly described|p129, p132 Fig.2-131, p133 Tb.2-16|||See also p152 Tb.2-22. Formerly part of Friendly Creek Formation (of Fitton et al., 1975) and part of Chocolate Hill Formation (Ingram, 1977). Chromium/nickel rich indicates ultramafic origin. 100m thick.||Talga Talga Subgroup|||Carbonate-chlorite-quartz schist; chert, commonly ferruginous; some local ultramafic rocks.|
26023|McPhee Formation|50381|5|Briefly described|Map Legend|Archean|Archean|Of Talga Talga Subgroup (Warrawoona Group). Geological Province: Pilbara Craton. Age: c. 3477 Ma.||||||07-NOV-08
26023|McPhee Formation|50427|5|Briefly described|p191|Archean|Archean|Talc-carbonate ultramafic schist.||||||07-NOV-08
26023|McPhee Formation|60636|5|Briefly described|p37, p55|Archean|Archean|Presented as McPhee only in text. Of the Warrawoona Group. Age: ~3469Ma. See also p119.||||||07-FEB-11
26023|McPhee Formation|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Geological Province: eastern Pilbara Craton.||||||07-NOV-08
26023|McPhee Formation|61266|5|Briefly described|p58 Tb.1|Archean|Archean|Of the Talga Talga Subgroup (Warrawoona Group). Talc-chlorite schist, chert, BIF, pelite. Geological Province: Pilbara Craton.||||||07-NOV-08
26023|McPhee Formation|61579|5|Briefly described|p58 Fig. 2|Archean|Archean|Of the Warrawoona Group.||||||07-NOV-08
26023|McPhee Formation|62427|5|Briefly described|p4, p12 Fig.9, p17-18 |Paleoarchean|Paleoarchean|Another age of 3478 +/- 2 Ma inferred from Fig.9.|3469 +/- 3 Ma|Of the Warrawoona Group||||
26023|McPhee Formation|63420|5|Briefly described|Map legend|Archean|Archean|Of Talga Talga Subgroup (Warrawoona Group, Pilbara Supergroup).  Age: c3477Ma. Geological Province: Pilbara Craton. Ultramafic and mafic volcanic rocks, siliciclastic sedimentary rock and chert; metamorphosed.||||||07-NOV-08
26023|McPhee Formation|63441|5|Briefly described|p4 Tb. 1|Archean|Archean|Of Talga Talga Subgroup (Warrawoona Group, Pilbara Supergroup).||||||07-FEB-11
26023|McPhee Formation|63538|5|Briefly described|p6 Fig. 3|Archean|Archean|Of Warrawoona Group (Talga Talga Subgroup). Overlies North Star Basalt. Geological Province: Pilbara Craton. Basalt.||||||
26023|McPhee Formation|63649|5|Briefly described|p201 Fig. 2|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Age: 3.477Ga  Geological Province: Pilbara Craton.||||||07-FEB-11
26023|McPhee Formation|64328|5|Briefly described|p56 Tb. 1|||Of Talga Talga Subgroup (Warrawoona Group). Ultramafic rock, chert, felsic volcanic rocks.||||||07-FEB-11
26023|McPhee Formation|64405|5|Briefly described|p4 Fig. 3|Archean|Archean|Name inferred from McPhee only in Figure 3. Of the Warrawoona Group (De Grey Supergroup). Felsic rocks.||||||07-FEB-11
26023|McPhee Formation|64621|5|Briefly described|Map legend|Archean|Archean|Of Talga Talga Subgroup (Warrawoona Group, Pilbara Supergroup). Age: <c.3477Ma. Lithology details for at least 6 rock types included.||||||07-NOV-08
26023|McPhee Formation|64936|5|Briefly described|map legend|Archean|Archean|Of Talga Talga Subgroup. Over North Star Basalt; under Mount Ada Basalt. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
26023|McPhee Formation|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in upper Talga Talga Subgroup. Aged c. 3477 Ma. Ultramafic volcanic rocks, siliciclastic sedimentary rocks, basalt, and chert; local felsic volcanic rocks; metamorphosed.||||||
26023|McPhee Formation|66217|4|Described|p5, pp14-17, p35, p58, p60.|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. A lateral equivalent to the Dresser Formation. Thickness 100 m, up to 750 m. Hosts several gold prospects in the Marble Bar greenstone belt, and massive sulfides in the Warralong greenstone belt.|3477 +/- 2 Ma (U-Pb SHRIMP zircon: Nelson 2000a).|Uppermost unit in Talga Talga Subgroup.||Conformably overlies North Star Basalt. Is conformably overlain by Mount Ada Basalt.|Felsic volcaniclastic rocks; layered sedimentary chert including minor pelite and siliceous iron-formation; and carbonate-chlorite-quartz rock (metamorphosed ultramafic rock) that forms the bulk of the Formation.|
26023|McPhee Formation|66745|3|Fully described|p51, pp53-54, pp56-57.|Paleoarchean|Paleoarchean|Correlated with Dresser Formation. Crustal extension, with hydrothermal activity in thermal lakes (stromatolites). Base metal mineralization.|<3481-3477 Ma.|Unit in Talga Talga Subgroup.||Overlies North Star Basalt. Is disconformably overlain by Mount Ada Basalt.|Basalt, chert, carbonate rocks; minor felsic volcaniclastic rocks.|
26023|McPhee Formation|67130|6|Mentioned|p15 fig 10|Paleoarchean|Paleoarchean||3477 Ma|Warrawoona Group||Overlies North Star Basalt, overlain by Mount Ada Basalt|Felsic volcanic rocks.|
26023|McPhee Formation|67197|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Talga Talga Subgroup.||||
26023|McPhee Formation|67201|4|Described|p7 Fig.4, p12 Tb.1|||In northern Pilbara Craton, East Pilbara Terrane. Shown as McPhee and Dresser Fm.|c. 3480 Ma|Talga Talga Subgroup||||
26023|McPhee Formation|67269|5|Briefly described|p6 Fig.3|Paleoarchean|Paleoarchean||<3481-3477 Ma.|Talga Talga Subgroup.||||
26023|McPhee Formation|67270|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.|<3481-3477 Ma.|Talga Talga Subgroup.||||
26023|McPhee Formation|67668|6|Mentioned|Fig. 2;||Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Warrawoona Group||Underlies the Mount Ada Basalt, overlies the North Star Basalt. Dresser Formation.||
26023|McPhee Formation|68035|6|Mentioned|p288 Fig 4|Paleoarchean|Paleoarchean|Warrawoona Group, Pilbara Supergroup, East Pilbara Terrane. Shown as McPhee and Dresser Formations (<3481-3477 Ma).||Of Talga Talga Subgroup.||Overlies North Star Basalt? Disconformably overlain by Mount Ada Basalt.||
26023|McPhee Formation|68280|6|Mentioned|p4|||||Talga Talga Subgroup||Disconformably overlain by Mount Ada Basalt, overlies North Star Basalt|Chert and felsic volcanic rocks.|
26023|McPhee Formation|68281|6|Mentioned|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Warrawoona Group.||||23-SEP-13
26023|McPhee Formation|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c.3477 Ma|Of the Talga Talga Subgroup.|||Ultramafic and mafic volcanic rocks, siliciclastic sedimentary rock, and chert; metamorphosed.|
26023|McPhee Formation|68284|5|Briefly described|p7|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Talga Talga Subgroup.||Overlies North Star Basalt. Is overlain by Mount Ada Basalt.||
26023|McPhee Formation|69012|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane.|c. 3477 Ma|Of the Talga Talga Subgroup.||||
26023|McPhee Formation|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Mapped as 4 unnamed sub-units.|c. 3477 Ma|Of the Talga Talga Subgroup.|||Metachert; fine- to medium-grained amphibolite, locally schistose, metamorphosed basalt; carbonate-altered mafic volcanic rock and derived mafic schist; talc-chlorite schist, metamorphosed ultramafic rocks.|02-MAY-14
26023|McPhee Formation|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Chert, and local banded iron formation, basalt - massive or pillowed, komatiitic basalt, pillowed komatiitic basalt. Age derived from chert sample with a volcanigenic component- age is of this volcanic component(148498.1.pdf)|3477 Ma +/- 2 Ma (SHRIMP)|Talga Talga Subgroup|||Basalt, and chert; metamorphosed. Amphibolite, carbonate altered mafic volcanic rock, mafic schist, talc chlorite schist, talc carbonate and chlorite-serpentine-carbonate schist.|
26023|McPhee Formation|69301|4|Described|p5 Fig.3, p9 Tb.1, p20 Tb.2|||Pilbara Craton. East Pilbara Terrane. Shown as McPhee and Dresser Fm.|<3481-3477 Ma; 3480 Ma McPhee&Dresser Formations|Talga Talga Subgroup||Disconformity at top of McPhee Formation and Dresser Formation.|Banded-iron formation, felsic volcanic rocks.|
26023|McPhee Formation|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA (green-grey chert with silty tuffaceous layers) yielded an interpreted igneous crystallisation age of 3477+\-2 Ma for the volcanigenic component in the chert. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.|477 Ma (isotopic)|Unit of Talga Talga Subgroup.|||Banded iron-formation, layered and ferruginous chert; metamorphosed; massive, pillowed or komatiitic basalt, mafic volcanics, altered schist; metamorphosed ultramafic volcanics, siliciclastic sedimentary rocks.|
26023|McPhee Formation|70022|6|Mentioned|p115|||East Pilbara Terrane.||Talga Talga Subgroup.||||
26023|McPhee Formation|70775|5|Briefly described|p12|Paleoarchean|Paleoarchean|East Pilbara.|c. 3480 Ma|Warrawoona Group||Overlies the North Star Basalt. Overlain by the Mount Ada Basalt.||
26023|McPhee Formation|70834|6|Mentioned|p298|Paleoarchean|Paleoarchean|Marble Bar greenstone belt, Pilbara Craton.|3477 Ma.|||Overlies North Star Basalt. Is overlain by Mount Ada Basalt.|Komatiite, chert.|
26023|McPhee Formation|70884|5|Briefly described|p123-124|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|c. 3.48 Ga|Unit of Talga Talga Subgroup.||Overlain by Mount Ada Basalt/Coongan Subgroup. Underlain by Dresser Formation.||
26023|McPhee Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Warrawoona  Large Igneous Province.|3477+/-2 Ma.|Talga Talga Subgroup|||Ultramafic volcanic rock, siliciclastic sedimentary rock, basalt, and chert; local felsic volcanic rock; metamorphosed.|
26023|McPhee Formation|72064|5|Briefly described|p66|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawoona Group.||Overlain unconformably by Mount Ada Basalt. Underlain by Dresser Formation.||
26023|McPhee Formation|72251|5|Briefly described|p54|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Talga Talga Subgroup.||Overlain by Mount Ada Basalt. Underlain by North Star Basalt.||
26023|McPhee Formation|72668|6|Mentioned|p4-6, p17|||East Pilbara Terrane. No name ending shown in figures p4,5. Lithology uncertain, but implied to be felsic. Shown as McPhee Formation p17.|c. 3477 Ma.|Talga Talga Subgroup||Overlies the North Star Basalt.||13-JAN-22
26023|McPhee Formation|73598|6|Mentioned|p1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Talga Talga Subgroup.||Overlies North Star Basalt. Is overlain by Mount Ada Basalt.||
29292|McSherrys Granodiorite|23722|6|Mentioned|p12|||||||||
29292|McSherrys Granodiorite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1860Ma. Geological province: Kimberley Province (West).||||||07-FEB-11
29292|McSherrys Granodiorite|30525|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
29292|McSherrys Granodiorite|30533|4|Described|p13|||On Table 1||||||
29292|McSherrys Granodiorite|30895|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
29292|McSherrys Granodiorite|36885|4|Described|p175|||||||||
29292|McSherrys Granodiorite|41158|6|Mentioned|Plate 2|||||||||
29292|McSherrys Granodiorite|41987|5|Briefly described|p73|||||||||
29292|McSherrys Granodiorite|42149|6|Mentioned|p710|||||||||
29292|McSherrys Granodiorite|42710|5|Briefly described|map legend|Proterozoic||||||||17-OCT-12
29292|McSherrys Granodiorite|42811|5|Briefly described|p11|||||||||
29292|McSherrys Granodiorite|42814|6|Mentioned|p9|||||||||
29292|McSherrys Granodiorite|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|Approx 1865 - 1850 Ma.||||||
29292|McSherrys Granodiorite|43666|6|Mentioned|p52,Table 2||Neoproterozoic|||||||
29292|McSherrys Granodiorite|43819|6|Mentioned|Table 2,p33|||||||||
29292|McSherrys Granodiorite|44155|4|Described|p241, p242 Tb.3-5, p248 Tb.3-8|||West Kimberley. Cut by abundant dolerite and aplite dykes, trending NW to NNW, that are undeformed and unaltered.||Hooper Complex||Is intruded by Lennard Granite and Dyason Granite.|Grey, mesocratic porphyritic biotite-hornblende granodiorite and tonalite; minor monzogranite and quartz gabbro; granodiorite and granite xenoliths common.|
29292|McSherrys Granodiorite|50437|5|Briefly described|p1.5, 2.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite. Age: 1862 +/- 4Ma (Shrimp).||||||07-NOV-08
29292|McSherrys Granodiorite|60533|5|Briefly described|p604|Paleoproterozoic|Paleoproterozoic|Age: 1861 +/- 4Ma (Griffin et al, 2000).||||||07-NOV-08
29292|McSherrys Granodiorite|63866|5|Briefly described|p132|||Western Zone, Halls Creek Orogen.|c. 1862 Ma|Paperbark Supersuite||||
29292|McSherrys Granodiorite|69099|5|Briefly described|ga_geochron.csv|||King Leopold Inlier. Data migrated from OZCHRON1. Original comment: 'This is the age of igneous crystallisation of the McSherrys pluton.'|1862+/-4 Ma SHRIMP|||||03-AUG-15
29292|McSherrys Granodiorite|69165|6|Mentioned|GA_geochron.csv|Paleoproterozoic|Paleoproterozoic||1862 Ma|||||
29292|McSherrys Granodiorite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Paperbark Supersuite.|||Foliated porphyritic to even grained biotite hornblende granodiorite and tonalite with minor monzogranite and abundant small mafic xenoliths|
29292|McSherrys Granodiorite|72437|5|Briefly described|p65, p73|||Hooper Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Granodiorite.|
26024|Meda Formation|7433|5|Briefly described|p25 Fig.2, p42, p44. |Jurassic|Jurassic|Fitzroy Sub-basin, Canning Basin. Fluvial clastics. Forms isolated thin cappings to hills of Triassic rocks. Possible equivalent to Barbwire Sandstone.|||||Well-rounded, pebble conglomerate, coarse sandstone.|
26024|Meda Formation|22776|4|Described|p11, Table.3|Early Cretaceous|Jurassic|Also p21.||||||
26024|Meda Formation|32648|6|Mentioned|p32|||Lower Cretaceous.||||||
26024|Meda Formation|34008|6|Mentioned|p70|||L.Cret.||||||
26024|Meda Formation|36224|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Sandstone, granule to pebble conglomerate.||||||01-FEB-05
26024|Meda Formation|36890|3|Fully described|p353|||||||||
26024|Meda Formation|38263|6|Mentioned|p13|||||||||
26024|Meda Formation|38878|6|Mentioned|Map legend|Kimmeridgian|Oxfordian|Oxfordian - Kimmeridgian||||||
26024|Meda Formation|41688|4|Described|p15|||||||||
26024|Meda Formation|43281|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|||||||
26024|Meda Formation|44143|4|Described|p.433 Table 4-19|Jurassic|Jurassic|Up to 9m thick; fine to coarse sandstone; granule and pebble conglomerate; fluvial. Unconformably overlies Erskine Sandstone. Type section at Erskine Range (DERBY: 17deg 50' S, 124deg 22' E). Contains wood fragments.||||||
26024|Meda Formation|44998|2|Defined|p145||Jurassic|Overlies Erskine Sandstone. (E51-7). See also p115,133,143 - 185, map.||||||
26024|Meda Formation|45153|2|Defined|App.6-117|Early Cretaceous|Early Cretaceous|See also App.5-89||||||
26024|Meda Formation|45158|3|Fully described|p14|||||||||
26024|Meda Formation|48826|14|Not recorded|Tb.III|||Correlates with Godfrey Beds.||||||
26024|Meda Formation|68811|6|Mentioned|p80|||Along with Wallal Sandstone, hosts the Wallal aquifer.||||||15-APR-20
26024|Meda Formation|70826|6|Mentioned|p7 tbl 4|Early Cretaceous|Jurassic|Canning Basin.||||||
26024|Meda Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Sandstone, granule to pebble conglomerate.|
74805|Meekatharra Formation|64891|5|Briefly described|p37 Fig.2, p39-40, p48-9 Tb. 1|Archean|Archean|Of the Polelle Group. Age: 2800-2760Ma; 2784+/-22Ma (for a basal dacite). Geological province: Murchison Domain. Basalt and komatiitic basalt; metamorphosed.||||||07-FEB-11
74805|Meekatharra Formation|65546|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Polelle Group, Youanmi Terrane, Yilgarn Craton. 2800-2760 Ma.Strongly foliated metabasalt and amphibolite; meta pyroxene spinifex textured basalts; locally schistose basalt; massive to weakly foliated; locally pillowed and/or vesicular; metamorphosed.||||||
74805|Meekatharra Formation|65548|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Polelle Group, Youanmi Terrane, Yilgarn Craton. 2800-2760 Ma.  Basalt, massive to weakly foliated locally pillowed and/or vesicular, metamorphosed; pyroxene spinifex-textured basalts; locally variolitic, metamorphosed||||||
74805|Meekatharra Formation|65550|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Polelle Group, Murchison Supergroup, Murchison Domain. Age shown as 2800-2760 Ma. Consists of mainly sedimentary rocks, felsic volcanic rocks, and basalt, metamorphosed.||||||18-AUG-10
74805|Meekatharra Formation|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Mapped as nineteen separate but un-named units.|2800 - 2760 Ma.|Unit in Polelle Group.|||Komatiitic basalt +/- pillowed; pyroxene spinifex-textured basalt; fine-grained ultramafic schist; metakomatiitic basalt; mylonitic metabasalt; amphibolite schist and gneiss; felsic volcaniclastic siltstone; schistose pelite and psammite.|
74805|Meekatharra Formation|67129|6|Mentioned|p18 fig 19, p20, p33, p47|Archean|Archean|Murchison Domain, Youanmi Terrane. Geochemical modelling.|c.2790 Ma.|Polelle Group|Stockyard Basalt Member, Lordy Basalt Member.||Komatiites, mafic - ultramafic volcanics, basalts.|07-SEP-17
74805|Meekatharra Formation|68107|6|Mentioned|p618|||||Of the Polelle Group.|||Mafic volcanics.|
74805|Meekatharra Formation|68110|4|Described|p673, p674 Fig.2|Neoarchean|Neoarchean|Murchison Domain. A dacite near the base of this formation has an age of 2784 +/- 22 Ma.|c. 2792-2761 Ma|Basal unit of the Polelle Group.|Includes Stockyard Basalt and Lordy Basalt.|Conformably overlies Yaloginda Formation (Norie Group). Conformably overlain by the Greensleeves Formation.|Basalt, komatiitic basalt, komatiite; minor dacite, felsic volcaniclastics.|
74805|Meekatharra Formation|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane||Polelle Group|Includes 22 unnamed subunits.|Conformably overlain by Greensleeves Formation.|Schistose pelite and psammite; Shale and mudstone with volcaniclastic rock; Felsic volcaniclastic siltstone; Amphibolite; Metamafic rock; Amphibolite gneiss; Amphibolite schist; Metabasalt;  ultramafic schist;|23-OCT-15
74805|Meekatharra Formation|68698|5|Briefly described|p4-5, p7, p9, p17, p33-34|Neoarchean|Neoarchean|Geochemistry is discussed.|c.2800-2760 Ma.|Polelle Group.||Overlies Coodardy Formation. Is overlain by Woolgra Andesite Member (Greensleeves Formation).|Dominantly tholeiitic basalt, komatiitic basalt, komatiite, and thin interflow felsic volcaniclastic sedimentary rocks.|
74805|Meekatharra Formation|69014|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. 6 unnamed facies, mapped separately.|2800-2760 Ma|Of the Polelle Group.|||Massive to weakly foliated basalt; komatiitic basalt; pyroxene spinifex-textured basalt; metakomatiitic basalt with local hyaloclastite; tremolite-chlorite(-talc) schist; shale and mudstone with volcaniclastic rock; all metamorphosed.|01-MAY-14
74805|Meekatharra Formation|69583|4|Described|p47, p49, p126; Plate 2|Neoarchean|Neoarchean|Murchison Domain.|c.2800-2760 Ma.|Polelle Group.|Lordy, Stockyard, Basalt Members.|Is overlain by Glen Group.|Dominantly tholeiitic basalt, komatiitic basalt, komatiite and thin interflow volcaniclastic sedimentary rocks; BIF and felsic volcaniclastic rock; weakly metamorphosed.|
74805|Meekatharra Formation|69584|5|Briefly described|p5 Fig.2, p54|Neoarchean|Neoarchean|||Polelle Group|Lordy Basalt, Stockyard Basalt|Overlies the Coodardy and Mougooderra Formations. Overlain by the Greensleeves Formation.|Basaltic rocks.|
74805|Meekatharra Formation|69586|5|Briefly described|p21-23, p31 Fig.33|Neoarchean|Neoarchean||c.2800-2760 Ma.|Polelle Group.|Lordy, Stockyard, Basalt Members.||Includes tholeiitic and komatiitic basalts.|
74805|Meekatharra Formation|69627|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Detailed lithology in legend. |2800-2760 Ma|Polelle Group|||Schistose pelite and psammite; meta BIF; amphibolite (schist) derived from basalt; (meta)komatiitic basalt and ultramafic schist; basalt; talc-carbonate(-chlorite-serpentine) schist derived from komatiitic rocks.|
74805|Meekatharra Formation|69628|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton|2800-2760 Ma|Polelle Group|||Komatiitic basalt; locally pillowed and/or variolitic; fractured to locally foliated; weakly metamorphosed.|
74805|Meekatharra Formation|69744|6|Mentioned|p259|||Mount Magnet Greenstone Belt.||||||
74805|Meekatharra Formation|70020|4|Described|p117-118|Neoarchean|Neoarchean|Geological province: Yilgarn Craton. Thickness: 2.5 km.||Unit of Polelle Group.||Overlain by Greensleeves Formation. Underlain by Coodardy/Mougooderra Formation.|Tholeiitic basalt, komatiitic basalt, komatiite and thin interflow 2800-2760 Ma felsic volcaniclastic sedimentary rocks.|
74805|Meekatharra Formation|70139|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton. No fewer than 19 facies are mapped separately.|2800-2760 Ma.|Polelle Group.|||Quartzite; felsic, metarhyolitic, mafic amphibolite schists; metabasalt, locally interleaved with meta-BIF; ultramafic schist; pyroxene spinifex-textured metabasalt; weakly metamorphosed komatiitic and pillowed basalts; amphibolite; volcaniclastics.|
74805|Meekatharra Formation|70418|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Polelle Group.|||Massive to weakly foliated, metamorphosed basalt, locally pillowed and/or vesicular; fine-grained ultramafic schist, local talc-carbonate rock, commonly deeply weathered; amphibolite after basalt, massive to foliated and/or lineated.|
74805|Meekatharra Formation|70796|5|Briefly described|100k_geologyl_lut.csv|Neoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 183338.1.pdf, 185920.1.pdf, 185932.1.pdf, Austin100_2442_stratig.pdf, Cue100_2443_stratig.pdf, Koonmarra100_2445_stratig.pdf, Madoonga100_2444_stratig.pdf, MountMagnet100_2441_stratig.pdf, Nowthanna100_2643_stratig.pdf, Reedy100_2543_stratig.pdf, Tieraco100_2545_stratig.pdf, Wynyangoo100_2542_stratig.pdf. Numerous additional lithologies are discussed.|ca 2800 to 2760 Ma (inferred)|Polelle Group|||Quartzite, schistose pelite and psammite, metamorphosed bandediron formation, felsic schist, amphibolite, metakomatiite basalt breccia, ultramafic schist, shale, mudstone, volcaniclastic rocks, and rhyolite.|
74805|Meekatharra Formation|70830|5|Briefly described|p7, p9, p14|||||Polelle Group||Overlies the Coodardy Pool Formation. Overlain by the Greensleeves Formation.|Tholeiitic basalt, komatiitic basalt, komatiite and thin interflow felsic volcaniclastic sedimentary rocks.|
74805|Meekatharra Formation|71168|5|Briefly described|p7-p8|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. 2.5km thick.|c. 2790-2760 Ma|Polelle Group||Overlies the Coodardy Formation and the Mougooderra Formation. Overlain by the Greensleeves Formation.|Komatiite, komatiitic basalt, tholeiitic basalt and thin interflow felsic volcaniclastic sedimentary rocks.|
74805|Meekatharra Formation|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeol_lut.csv.|2800-2760 Ma|Unit of Poelle Group.|Includes Bassetts Volcanic Member, Lordy Basalt Member, Stockyard Basalt Member.|Underlain conformably by Meekatharra Formation.|Schistose pelite, psammite; schist: metarhyolite, felsic, mafic derived from amphibolite; basalt: pillowed, komatiitic, pyroxene spinifex, mylonitic, metakomatiitic, BIFs; amphibolite gneiss; mafic volcanics, felsic volcaniclastics.|
74805|Meekatharra Formation|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.||Polelle Group.|Lordy Basalt Member, Bassetts Volcanic Member, Stockyard Basalt Member.||Felsic, mafic and amphibolite schists, metabasalts, metasedimentary rocks: 14 unnamed facies are each mapped separately.|
74805|Meekatharra Formation|71311|5|Briefly described|p795|||Mount Magnet greenstone belt area.|||||Greenstones.|
74805|Meekatharra Formation|71809|5|Briefly described|map legend|Archean|Archean|Yilgarn Craton, Youanmi Terrane||Of Polelle Group.|||Quartzite and psammite; Metamorphosed banded iron-formation + banded chert; Tremolite-chlorite(-talc) schist; Rhyolite;  local hyaloclastite; Basalt; interlayered w thin sills of granophyric to coarse-grained leucogabbro; all metamorphosed.|
74805|Meekatharra Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Mesoarchean|Youanmi Terrane. ||Polelle Group|||Basalt and komatiitic basalt; minor felsic volcanic rocks; generally weakly metamorphosed.|
74805|Meekatharra Formation|72389|5|Briefly described|Map Legend|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Gabanintha 1:100k map sheet 2644. Includes numerous unnamed constituents.|2800-2780 Ma|Polelle Group|Includes the Stockyard Basalt Member, Bassetts Volcanic Member and the Lordy Basalt Member.||Felsic schist, metamorphosed ultramafic rock, metamorphosed sedimentary rock, metamorphosed mafic rock, pillowed basalt, pillowed komatiitic basalt.|28-AUG-20
74805|Meekatharra Formation|72494|5|Briefly described|p15|||Youanmi Terrane, Yilgarn Craton.||Polelle Group.||Conformably overlies the Norie Group. Is overlain conformably by Greensleeves Formation.|Tholeiitic basalts, pyroxene spinifex-textured siliceous high magnesium basalts and boninites, locally interbedded with minor felsic volcanic and volcaniclastic units.|
74805|Meekatharra Formation|73410|6|Mentioned|p8 Fig.8||||c.2800-2760 Ma.||||Includes vesicular basalt.|
74805|Meekatharra Formation|73596|6|Mentioned|p1170|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane.|2799 +/- 2 Ma.|Polelle Group.||||
74822|Meeline Suite|64891|4|Described|p37 Fig. 2, p42, p50-51 Tb. 1|Archean|Archean|Of Annean Supers'te. Includes Youanmi, Windimurra, Lady Alma Barrambie+Atley Igneous Complexes. Age: c.2780Ma. Geol.prov: Murch.Dom.Mafic+ultra-mafic layered intrusive rocks - dominantly gabbros with anorthosite, magnetite and ultramafic cumulate rocks||||||07-FEB-11
74822|Meeline Suite|66195|4|Described|p601, p605,609, Fig.3, p598, p599 Fig.2|Neoarchean|Mesoarchean|Yilgarn Craton. Comprises the Windimurra, Youanmi, Barrambie, Lady Alma and Atley Igneous Complexes which intrude the Norie Group. Gabbroic with abundant leucogabbro and magnetitite.|Maximum age </= 2815 Ma.||||Gabbroic with abundant leucogabbro and magnetitite.|13-MAR-12
74822|Meeline Suite|67129|5|Briefly described|p18 Fig.19, p19 Fig.20, p20, p51-54|Archean|Archean|See also p57, p60. Hosts significant vanadium mineralization and some chromium, nickel, copper and PGE mineralization.|c.2810 Ma.|Annean Supersuite|Windimurra, Youanmi, Atley, Lady Alma, Barrambie, Igneous Complexes.||Mafic-ultramafic rocks.|07-SEP-17
74822|Meeline Suite|68107|6|Mentioned|p618||||c.2800 Ma (Van Kranendonk and Ivanic, 2009).||||Mafic and ultramafic layered intrusions.|
74822|Meeline Suite|68108|4|Described|p650, p651 Tb.4|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane. Includes the Windimurra (layered) intrusion.|ca. 2810 Ma; U-Pb (Ivanic et al. 2010)||Includes Windimurra Igneous Complex.||Differentiated igneous complexes.|
74822|Meeline Suite|68110|5|Briefly described|p686|Neoarchean|Mesoarchean|Murchison Domain. Appears as Meeline Mafic-Ultramafic Suite on p673, p674 Fig.2. Coeval with Norie Group; linked with plume-related crustal rifting?|c.2815 - 2000 Ma.||Includes Windimurra Igneous Complex.|||10-OCT-14
74822|Meeline Suite|68287|5|Briefly described|Map Legend|Archean|Archean|Metamorphosed.||Of the Annean Supersuite.|Includes Windimurra Igneous Complex.|||
74822|Meeline Suite|68519|5|Briefly described|Map Legend|Neoarchean||Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Of the Annean Supersuite.|Includes Windimurra Igneous Complex and Atley Igneous Complex.|||
74822|Meeline Suite|68561|5|Briefly described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane. See geochron file 194747.1.pdf.|~2810 Ma|Annean Supersuite|Includes Barrambie Igneous Complex, Atley Igneous Complex, Youanmi Igneous Complex,  Lady Alma Igneous Complex, Windimurra Igneous Complex|Intrudes  Norie Group.|layered mafic-ultramafic intrusions|
74822|Meeline Suite|68698|5|Briefly described|p4-5, p9, p18|Mesoarchean|Mesoarchean|Coeval with Norie Group volcanism. A vast intrusive igneous complex produced by a proposed plume event, and followed by mafic-ultramafic volcanism (eg Polelle Group). Up to 7km thick and 80km diameter. Contains V and minor Cu-Ni-PGE mineralisation.|c.2815 Ma.|Annean Supersuite.|||Very large layered mafic-ultramafic igneous complex.|
74822|Meeline Suite|69014|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane.||Of the Annean Supersuite.|Includes the Windimurra Igneous Complex.|||
74822|Meeline Suite|69583|4|Described|p47, p49-50, p54, p56, p97-98, p101-102|Mesoarchean|Mesoarchean|See also p168, p176-177; Plate 2. Murchison Domain, western Youanmi Terrane. The type example is the Windimurra Igneous Complex. Emplacement was accompanied by Norie Group volcanism. All five constituent complexes are >3km thick. Geological map. Igneous stratigraphic column. The Border, Ultramafic, Lower, Middle, Upper and Roof Zones are mapped separately in Plate 2. Prospective for Cu, Ni, Cr and PGEs.|c.2820 - 2810 Ma.|Murchison Supergroup and Annean Supersuite.|Atley, Barrambie, Buddadoo, Fields Find, Lady Alma, Wadgingarra, Windimurra, Youanmi, Igneous Complexes.||Consists of five large, layered mafic-ultramafic igneous complexes. Composition ranges from dunite through to anorthosite with thick layers of magnetite.|
74822|Meeline Suite|69584|6|Mentioned|p2|Mesoarchean|Mesoarchean||c. 2810 Ma||Youanmi, Windimurra, Atley, Barrambie, Lady Alma, Fields Find, Buddadoo and Wadgingarra, Igneous Complexes.|Intrudes the Norie Group||
74822|Meeline Suite|69586|5|Briefly described|p22|Mesoarchean|Mesoarchean|Murchison Domain.|||Windimurra, Youanmi, Atley, Barrambie, Lady Alma, Fields Find, Buddadoo, Wadgingarra, Igneous Complexes.|||
74822|Meeline Suite|69626|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton||Annean Supersuite|Windimurra Igneous Complex|||
74822|Meeline Suite|69628|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton|c. 2810 Ma|Annean Supersuite|Barrambie Igneous Complex, Lady Alma Igneous Complex|||
74822|Meeline Suite|70020|5|Briefly described|p113,118,120,128-129|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton. Comprises felsic rocks hosting VHMS mineralisation. |||||Komatiite and komatiitic basalt.|
74822|Meeline Suite|70030|5|Briefly described|p190|||Geological province: Murchison Domain, Yilgarn Craton. Mafic intrusive associated with Norie Group (Ivanic et al., 2010).||||||
74822|Meeline Suite|70140|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Annean Supersuite.|Youanmi and Windimurra, Igneous Complexes.|||
74822|Meeline Suite|70332|6|Mentioned|p77|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|||Youanmi Igneous Complex.||Anhydrous.|
74822|Meeline Suite|70419|5|Briefly described|p1-3, p7-8|Mesoarchean|Mesoarchean|Ivanic et al. (2010). Yilgarn Craton. Plume-related and laterally extensive.|c.2813 Ma.||Windimurra, Youanmi, Lady Alma, Atley, Barrambie Igneous Complexes.|Intrudes the Norie Group.|An anhydrous tholeiitic suite comprising five layered mafic-ultramafic intrusions.|
74822|Meeline Suite|70420|5|Briefly described|p2|||Southern Cross Domain, Youanmi Terrane, Yilgarn Craton.|||Barrambie Igneous Complex.||Mafic-ultramafic layered intrusions.|
74822|Meeline Suite|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton.|c.2813 Ma.|Annean Supersuite.|Buddadoo Gabbro.|||
74822|Meeline Suite|70770|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c.2813 Ma.||Windimurra Igneous Complex.|||
74822|Meeline Suite|70796|4|Described|2_5m_interpgeop15_lut.csv|Mesoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. Affected by the Yilgarn Craton granite magmatism (3010  2600 Ma); Youanmi Terrane events (3131  2600 Ma). See also 100k_geologyl_lut.csv, 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 185995.1.pdf, 194747.1.pdf, 194749.1.pdf, 194751.1.pdf, 198210.1.pdf, Badja100_2240_stratig.pdf, Bungar100_2539_stratig.pdf, Challa100_2541_stratig.pdf, Nowthanna100_2643_stratig.pdf, Windimurra100_2641_stratig.pdf, Wynyangoo100_2542_stratig.pdf, Youanmi100_2640_stratig.pdf. Numerous additional lithologies are discussed.|ca 2819 to 2813 Ma (inferred)|Annean Supersuite|Includes the Youanmi Igneous Complex.|Intruded by the Mount Kenneth Suite.|Layered maficultramafic intrusive rocks; gabbro with subordinate anorthosite, magnetitite, and ultramafic cumulate rocks; metamorphosed|
74822|Meeline Suite|70826|6|Mentioned|p8|Mesoarchean|Mesoarchean|Coincides with the deposition of the Norie Group.||||||
74822|Meeline Suite|70830|4|Described|p2-p5, p9, p25-p27, p50-p52|Neoarchean|Neoarchean|Murchison Domain. Consists of six large, layered mafic-ultramafic complexes. This unit is approximately 300km long with an estimated volume of 38000 km^3. Hosts rich vanadium mineralisation.|c. 2810 Ma|Annean Supersuite||Intrudes the Norie Group.|Mafic and ultramafic rocks including dunite through to anorthosite.|
74822|Meeline Suite|71159|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.||Annean Supersuite.|Windimurra Igneous Complex.|||
74822|Meeline Suite|71168|5|Briefly described|p7, p19 fig 11|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. See also p21-p22, p59-61.|c. 2810 Ma||Includes the Windimurra, Yoanmi, Atley, Barrambie, Lady Alma and Buddadoo Igneous complexes.||Large ultramafic-mafic intrusions. Granitic rocks.|
74822|Meeline Suite|71269|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Includes the Barrambie, Atley, Youanmi, Lady Alma and Windimurra Igneous Complexes (layered mafic-ultramafic intrusions). Sample GSWA 194747 (metagabbro from Windimurra Igneous Complex) yielded a weighted mean 207Pb/206Pb date of 2813+\-3 Ma, interpreted as the magmatic crystallization age of the gabbro protolith. Sample GSWA 194749 (metagabbronorite from Windimurra Igneous Complex) yielded a weighted mean 207Pb/206Pb date of 2802+\-19 Ma, tentatively interpreted as the magmatic crystallization age of the gabbroborite protolith; or a discordia upper intercept age of 2823+\-37 Ma. Sample GSWA 194751 (metadolerite from Youanmi Igneous Complex) yielded a concordia age of 2825+\-7 Ma, tentatively interpreted as maximum crystallisation age of the dolerite (representing inherited zircons from an older source). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|2819-2813 Ma (inferred0|Unit of Annean Supersuite.|Includes Buddadoo Gabbro, Corner Well Gabbro.|Intruded by Mount Kenneth Suite. Intrudes into Norie Group/Murchison Group.|Layered mafic--ultramafic intrusive rocks; gabbro with subordinate anorthosite, magnetitite, and ultramafic cumulate rocks; metamorphosed|
74822|Meeline Suite|72034|6|Mentioned|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Barrambie Igneous Complex.|||
74822|Meeline Suite|72389|5|Briefly described|Map Legend|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Gabanintha 1:100k map sheet 2644.||Annean Supersuite|Includes the Lady Alma Igneous Complex.|||28-AUG-20
38680|Meelup granite|23788|6|Mentioned|p36|||||||||
36836|Meentheena Member|23570|5|Briefly described|p237 Appendix 1|||Abbreviation of Meentheena Carbonate Member of Tumbiana Formation.||||||
36836|Meentheena Member|23575|5|Briefly described|Map Legend|Archean|Archean|Of Tumbiana Formation.||||||07-NOV-08
36836|Meentheena Member|24352|6|Mentioned|Map legend|Archean|Archean|Parent: Tumbiana Formation.  Age: >2717Ma.   Geological Province: Hamersley Basin||||||07-NOV-08
36836|Meentheena Member|24353|5|Briefly described|p23|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
36836|Meentheena Member|24554|5|Briefly described|p13|||Overlies the basalt component of the Tumbiana Formation.||||||
36836|Meentheena Member|50146|5|Briefly described|Map Legend|Archean|Archean|Of the Tumbiana Formation (Fortecsue Group). Geological Province: Hamersley Basin. Dark grey stromatolitic dolomite and limestone, carbonate-rich tuff, mudstone, and siltstone.||||||07-NOV-08
36836|Meentheena Member|50300|5|Briefly described|Map Legend|Archean|Archean|Of the Tumbiana Formation.  Geological Province: Hamersley Basin.||||||07-NOV-08
36836|Meentheena Member|50381|5|Briefly described|Map Legend|Archean|Archean|Of Tumbiana Formation (Fortescue Group). Geological Province: Hamersley Basin, Pilbara Craton.||||||07-NOV-08
36836|Meentheena Member|63372|4|Described|Map Legend|Archean|Archean|Of the Tumbiana Formation. Geological Province: Hamersley Basin. Dark grey stromatolitic dolomite and limestone, carbonate rich pyroclastic rocks, mudstone and siltstone. Over and underlain by Tumbiana Formation.||||||07-NOV-08
36836|Meentheena Member|64580|4|Described|map legend||Neoarchean|Of Tumbiana Formation. Lenses of stromatolitic dark-grey siliceous limestone or dolomite within volcaniclastic sandstone and siltstone (with accretionary lapilli), calcareous sandstone, shale, and basalt; local quartz sandstone and conglomerate.||||||15-DEC-08
36836|Meentheena Member|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Tumbiana Formation. Geological Province: Pilbara Craton. Carbonate rock.||||||07-FEB-11
36836|Meentheena Member|64654|5|Briefly described|Map Legend|Archaean|Archaean|Of Tumbiana Formation. Geological Province: Pilbara Craton (Hamersley Basin). Lenticular units of stromatolitic, dark-grey siliceous limestone or dolomite within laterally variable sequences of volcaniclastic sandstone and siltstone, calcareous sandstone.||||||
36836|Meentheena Member|64656|5|Briefly described|Map Legend|Archaean|Archaean|Of Tumbiana Formation.  Age: 2727-2721Ma. Geological Province: Hamersley Basin. Lenticular units of stromatolitic, dark-grey siliceous limestone or dolomite within laterally variable sequences of volcaniclastic sandstone and siltstone.||||||26-NOV-08
36836|Meentheena Member|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Tumbiana Formation. Geological Province: Hamersley Basin. Lenticular units of stromatolitic, dark-grey siliceous limestone or dolomite with laterally variable sequences of volcaniclastic sandstone and siltstone.||||||
36836|Meentheena Member|65008|5|Briefly described|p23, p41|||||Of the Tumbiana Formation||Underlain by the Mingah Member.|Banded dark-grey siliceous, stromatolitic dolomite and limestone beds, minor tuffaceous shale and siltstone, and rare thinly bedded tuff. Limestone contains scattered oncolites and stromatolites in bioherms and biostromes, and is oolitic in places.|14-MAY-14
36836|Meentheena Member|65724|5|Briefly described|map legend|Neoarchaean|Neoarchaean|Of Tumbiana Formation. Units of limestone or dolomite within sequences of volcaniclastic sandstone and siltstone, calcareous sandstone, shale and basalt; local quartz sandstone and conglomerate. Geol. Prov: Hamersley Basin, Pilbara Craton.||||||
36836|Meentheena Member|65726|5|Briefly described|Map legend|Archean|Archean|Hamersley Basin, Pilbara Craton.|c.2719 Ma (Blake 2001).|Of Tumbiana Formation.|||Banded dark-grey silicified limestone, dolomite, stromatolitic dolomite, and tuffaceous shale, siltstone and minor sandstone.|
36836|Meentheena Member|65727|5|Briefly described|Map legend|Neoarchean|Neoarchean|Fortescue Basin.||Of Tumbiana Formation.|||Lenticular units of stromatolitic siliceous limestone or dolomite with laterally variable sequences of volcaniclastic sandstone and siltstone, calcareous sandstone, shale, and basalt; local quartz sandstone and conglomerate.|
36836|Meentheena Member|65827|3|Fully described|p12 Tb.3, p33 Fig.6; p38, p40|Neoarchean|Neoarchean|Upper unit of Tumbiana Formation (Fortescue Group); formerly Meentheena Carbonate Member (Lipple, 1975). c. 2719 Ma. Shown as equivalent to part of Mount Jope Supersequence(1); overlies Mingah Member conformably. Lacustrine stromatolitic dolomitic carbonate and limestone.||||||
36836|Meentheena Member|65829|3|Fully described|p10, p15, p20, p22.|Neoarchean|Neoarchean|Formerly Meentheena Carbonate Member (Lipple 1975). A distinctive, commonly cliff-forming unit; the first thick carbonate unit marks its base. Non-stromatolitic carbonate beds may be oolitic, micritic, laminated and fenestrated. Contains a wide variety of sedimentary structures. Intruded by thick dolerite sills and dykes.|c.2719 Ma.|Unit in Tumbiana Formation.||Overlies conformably the Mingah Member.|Lenticular units of stromatolitic, dark grey siliceous limestone and dolomite with volcaniclastic sandstone and siltstone, including accretionary lapilli beds; with calcareous sandstone, carbonaceous shale, local quartz sandstone and conglomerate.|
36836|Meentheena Member|66685|4|Described|p215-238|Archean|Archean|Originally Meentheena Carbonate Member (Lipple, 1975). Pilbara Craton. 30-50 m thick. Type section 3 km NE of Pelican Pool. Highly detailed lithology, depositional models, numerous stratigraphic columns and REE + isotopic data. Authors conclude deposition occurred in a large lakes system. Base defined as first prominent, laterally persistent, limestone bed (usually a flat-pebble conglomerate).|~2720 Ma|Tumbiana Formation||Overlies the Mingah Member, usually conformably (and gradationally) but also unconformably.|Alternating limestone (dominant) and siliciclastic rock (shale, siltstone, and some sandstone with variable amounts of volcaniclastic material). Limestones are rich in sedimentary structures, with abundant and diverse stromatolites.|
36836|Meentheena Member|67201|5|Briefly described|p29 Fig.15|||In northern Pilbara Craton, Northern Fortescue Basin, Northeast Pilbara Sub-basin.||Tumbiana Formation||||
36836|Meentheena Member|67229|5|Briefly described|p2, p4-5, p7|Neoarchean|Neoarchean|Approx. 20m thick. Four lithofacies identified, indicating upward-deepening sequences; locally up to 25 vertical repetitions of these sequences indicating fluctuating water levels, possibly lacustrine. Stromatolites described in considerable detail.|||||Fine-grained, thinly laminated stromatolitic carbonate. The basal part is locally interbedded with basalt. Symmetrical ripples common; ooids locally present in calcareous sandstone.|
36836|Meentheena Member|68056|5|Briefly described|p171-172, 175-177, 181-186, 188, 190|Archean|Archean|Pilbara Craton. Intertidal or lacustrine deposits. Fe, C isotope data and pyrite shapes tabulated.||Tumbiana Formation.||Overlies Mingah Member. Is overlain unconformably by the Maddina Formation.|Stromatolitic limestones, carbonate-cemented sandstones, and siliceous mudstones (in ascending order). Sandstones and mudstones are tuffaceous.|
36836|Meentheena Member|69012|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.|2727-2715 Ma (Arndt et al 1991; Blake et al 2004)|Tumbiana Formation.|||Stromatolitic siliceous limestone and dolostone; interbedded with volcaniclastic sandstone and shale; local komatiitic basalt.|26-OCT-15
36836|Meentheena Member|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Tumbiana Formation|||Stromatolitic siliceous limestone and dolostone; interbedded with volcaniclastic sandstone and shale; local komatiitic basalt|
36836|Meentheena Member|69185|4|Described|500k_geologyp08_lut.csv||Neoarchean|Geological Province: Pilbara Craton.||Unit of Tumbiana Formation.|||Stromatolitic dark-grey siliceous limestone or dolomite lenses within laterally variable sequences of volcaniclastic sandstone and siltstone (with accretionary lapilli), calcareous sandstone, shale, and basalt; local quartz sandstone, conglomerate|
36836|Meentheena Member|69299|5|Briefly described|p19, map|Archean|Archean|Interpreted as a lacustrine unit (Awramik and Buchheim 2001). Geol. Prov: Hamersley Basin, Pilbara Craton.||Of Tumbiana Formation.|||Dark grey, siliceous, stromatolitic dolomite and limestone, carbonate-rich tuffaceous sedimentary rock, mudstone, and siltstone.|
36836|Meentheena Member|69301|5|Briefly described|p18 Fig.7|||Pilbara Craton. Fortescue Basin. Northeast Pilbara Sub-basin, Sequence 2.||Tumbiana Formation||||
36836|Meentheena Member|69411|4|Described|p282-283,285-286,288,291-293|Neoarchean|Neoarchean|Geological province: Pilbara Craton. Previously Meentheena Carbonate Member, and reassigned by Thorne and Hickman, 1998. Contains 0.2-1 m stromatolitic carbonate. Most likely deposited in a lacustrine environment (Awramik and Buchheim 2009), and corroborated by various geochemical studies (see p283 for references). May represent a series of disconnected ephemeral lakes with the distal elements of an inward draining continental basin (Nichols and Fisher, 2007).||Unit of Tumbiana Formation.||Underlain by Mingah Member.|Dark, prominently outcropping stromatolitic limestone and recessive shale, fine to medium grained carbonate, ripple cross-laminated calcareous sandstone, pebble conglomerate and finely laminated volcaniclastic units.|
36836|Meentheena Member|69590|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Of Northeast Pilbara Sub-basin, Fortescue Basin. Events: Pilbara Craton breakup. See 100k_geologyp_lut.csv, 100k_geologyl_lut.csv, 500k_geologyp08_lut.csv.|2727-2715 Ma (inferred)|Unit of Tumbiana Formation.|||Stromatolitic siliceous limestone and dolostone; interbedded with volcaniclastic sandstone and shale; local komatiitic basalt|
36836|Meentheena Member|69792|5|Briefly described|p1095, p1105-06|||Contains stromatolitic intervals in a suggested lacustrine environment. Shows frequent lateral facies changes; consists of lenticular units which cannot be traced laterally for more than a few kilometres.||Unit in Tumbiana Formation.||||
78757|Melita Formation|69631|5|Briefly described|p48-49|||Melita area.|||||Includes volcaniclastic sandstones and breccias, massive crystal-rich sandstone; local fine-grained vitric to variably crystal-rich sandstone; fragmental rhyolitic rocks; basalt and basaltic andesite; local accretionary lapilli, dolerite intrusions.|
78757|Melita Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Also includes felsic volcanic and volcaniclastic rocks.|2684 +/- 6 Ma (isotopic) - 2682 Ma (inferred).|Gindalbie Group.|||Quartz-muscovite schist, felsic schist, amphibolite, mafic schist, sandstone, siltstone, shale and chert; metamorphosed. Rhyolite to rhyodacite interleaved with basaltic to doleritic volcanics and intrusives. Dolerite, gabbro, peridotite.|
78757|Melita Formation|70773|5|Briefly described|p1, p64||||||||Volcaniclastic sandstone and oligomictic breccia of porphyritic rhyolite, volcanogenic sandstones and lesser fragmental rocks.|
78757|Melita Formation|71168|5|Briefly described|p35, p53|Neoarchean|Neoarchean|Ages provided are SHRIMP U-Pb zircon dates and may constrain the timing of nearby VMS mineralization at Jungle Pool.|c. 2683 Ma (Brown et al., 2002; Nelson, 1997c)|||||
78757|Melita Formation|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).  See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2684; 2681+\-2 Ma|Unit of Gindalbie Group.|||Volcanics and volcaniclastics: rhyolitic to rhyodacitic, poorly bedded tuffs and breccias, basalt, basaltic andesite, dolerite, gabbro; amphibolite, mafic schist, sandstone, siltstone, shale and chert; metamorphosed.|
31100|Melita Rhyolite|43478|2|Defined|p13-61|||||||||
78963|Melon Patch Granite|44155|5|Briefly described|p239 Tb.3-3, p248 Tb.3-8|Paleoproterozoic|Paleoproterozoic|East Kimberley.||Lamboo Complex||Intruded by Mabel Downs Granodiorite.|Even-grained biotite syenogranite and monzogranite; xenolith rich; folded and strongly foliated.|15-JAN-15
33665|Menangina Monzogranite|23786|5|Briefly described|p34 Tb. 4|||Geological Province: Yilgarn Craton.||||||
33665|Menangina Monzogranite|44203|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
33665|Menangina Monzogranite|60076|5|Briefly described|p23, p45 App. 1|Archean|Archean|[Agmmn]   Biotite monzogranite with prominent K-feldspar megacrysts; cut by pegmatite and aplite.||||||07-NOV-08
33665|Menangina Monzogranite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Biotite monzogranite with prominent K-feldspar megacrysts; cut by pegmatite and microgranite dykes.||||||07-FEB-11
33665|Menangina Monzogranite|69152|5|Briefly described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Biotite monzogranite with prominent K-feldspar megacrysts; cut by pegmatite and microgranitic dykes.|06-AUG-15
33665|Menangina Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Biotite monzogranite with prominent K-feldspar megacrysts; cut by pegmatite and microgranitic dykes.|
33665|Menangina Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
33665|Menangina Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. See 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv, 100k_geologysub10_lut.csv.|||||Biotite monzogranite with prominent K-feldspar megacrysts; cut by pegmatite and microgranitic dykes|
26027|Menzies Formation|22769|5|Briefly described|Table1p759|Pliocene|Holocene|||||||
26027|Menzies Formation|41199|2|Defined|p10|early Quaternary|late Tertiary|Reserved as Menzies.||||||19-FEB-08
26027|Menzies Formation|43065|6|Mentioned|p93|||||||||
31126|Mermaid Formation|13255|6|Mentioned|p369|Early Cretaceous|Early Cretaceous|Roebuck Basin.||||Overlies Broome Sandstone. Is overlain by Nelson Rocks Formation.||
31126|Mermaid Formation|43173|5|Briefly described|13|Early Cretaceous|Late Jurassic|||||||
31126|Mermaid Formation|44143|6|Mentioned|p449-450|Early Cretaceous|Early Cretaceous|Offshore facies equivalent of Broome Sandstone. Thickens gradually seaward.||||||
31126|Mermaid Formation|66193|5|Briefly described|p569 Fig.2|Early Cretaceous|Early Cretaceous|in offshore Canning Basin, overlies the Broome Sandstone, underlies Nelson Rocks Formation||||||
31126|Mermaid Formation|69297|6|Mentioned|p337, p352|Valanginian|Berriasian|Canning and Roebuck Basins. ||||Unconformably overlies the Baleine Formation; or overlies the Egret Foramtion. Overlain or interbedded with the Broome Sandstone. Overlain by the Nelson Rocks Formation.||
31126|Mermaid Formation|69689|6|Mentioned|p16|Cretaceous|Cretaceous|Roebuck Basin.||||Overlies Broome Sandstone. Is overlain by Nelson Rocks Formation.||
31126|Mermaid Formation|70065|5|Briefly described|Rowley: Fig.2; p2. Regional: Fig.4|Aptian|Berriasian|Roebuck Basin and offshore Canning Basin. Delta sands form reservoirs, while claystones form a regional seal.||||Overlies Baleine Formation. Encloses Broome Sandstone. Is overlain by Nelson Rocks Formation.||
80964|Mesozoic siliciclastic units, eastern Canning Basin 80964|72034|5|Briefly described|500k_interpgeop16_lut|Mesozoic|Mesozoic|Informal, eastern Canning Basin.|||||Siliciclastic rocks.|
27193|Metawandy Granite|23325|5|Briefly described|map legend|Precambrian|Precambrian|?Pilbara Craton.||||||
27193|Metawandy Granite|23570|5|Briefly described|p37|||Geological Province: Pilbara Craton||||||
27193|Metawandy Granite|34732|4|Described|p14|||Petrology.||||||
27193|Metawandy Granite|35218|2|Defined|p16|Neoarchean|Neoarchean|Appendix 3||||||07-NOV-08
27193|Metawandy Granite|37327|6|Mentioned|Fig.3|||||||||
27193|Metawandy Granite|40369|6|Mentioned|p7|||||||||
27193|Metawandy Granite|40905|6|Mentioned|Fig.1|||||||||
27193|Metawandy Granite|41843|6|Mentioned|p67|||||||||
27193|Metawandy Granite|41845|6|Mentioned|Fig. 1|||||||||
27193|Metawandy Granite|42260|6|Mentioned|p110|||||||||
27193|Metawandy Granite|44151|6|Mentioned|p163|||Named by Horwitz (1978). Forms the core of the Wyloo Dome.||||||
27193|Metawandy Granite|64580|4|Described|map legend||Mesoarchean|Monzogranite, locally abundant mafic xenoliths.||||||09-DEC-08
27193|Metawandy Granite|69028|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|2910-2830 Ma||||Monzogranite; locally abundant mafic xenoliths.|06-MAY-14
27193|Metawandy Granite|69166|5|Briefly described|500k_geologyp08_lut.csv|Mesoarchean|Mesoarchean||||||Monzogranite, locally abundant mafic xenoliths.|
27193|Metawandy Granite|69185|5|Briefly described|500k_geologyp08_lut.csv||Mesoarchean||||||Monzogranite, locally abundant mafic xenoliths|
27193|Metawandy Granite|70795|5|Briefly described|2_5m_interpgeop15_lut.csv|Mesoarchean|Mesoarchean|Also 500k_interpgeop14_lut.csv|2893 +/- 11 Ma||||Monzogranite; locally abundant mafic xenoliths.|
27193|Metawandy Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
27193|Metawandy Granite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Capricorn Orogen.|2893+/-11 Ma||||Monzogranite; locally abundant mafic xenoliths.|
27193|Metawandy Granite|72758|5|Briefly described|p3, p5-6, p17, p19, p28.|Archaean|Archaean|Occurs in the core of the Wyloo Dome. The southwestern margin of the granitoid is tectonized, dips approximately 45 degrees to the southwest, and is concordant with the layering in the adjacent rocks. p17 Table 1 shows Metwandy Granite as part of Pilbara Supergroup, but text p3, p5 does not support this.||||Intrudes Pilbara Supergoup. Unconformably underlies Fortescue Group. Cut by NW trending dolerite dyke.|Medium grained with an allotriomorphic granular texture that is partly recrystallized. Sericitized adamellite, locally strongly (cataclastically) deformed in part; large enclaves of mafic schist; mafic xenoliths locally abundant.|
27276|Meteorite Bore Member|23045|5|Briefly described|289|||Parent Turee Creek Group||||||
27276|Meteorite Bore Member|23046|6|Mentioned|177|||Parent Turee Creek Group||||||
27276|Meteorite Bore Member|23047|6|Mentioned|36 fig 2|||Of the Kungarra Formation. Hamersley Province. .||||||10-FEB-09
27276|Meteorite Bore Member|23280|5|Briefly described|Fig2p1086|||||||||
27276|Meteorite Bore Member|23890|5|Briefly described|p16|Paleoproterozoic|Paleoproterozoic|Of Kungarra Formation (Turee Creek Group).  Geological Province: Pilbara Craton. Maximum thickness: ~270m.||||||07-NOV-08
27276|Meteorite Bore Member|24544|5|Briefly described|p57 Fig.43|Paleoproterozoic|Paleoproterozoic|Of Kungarra Formation. Conglomerate. Geological Province: Hamersley Basin.||||||07-NOV-08
27276|Meteorite Bore Member|35976|2|Defined|p110|Proterozoic|Proterozoic|||||||
27276|Meteorite Bore Member|37934|3|Fully described|p555|||Member of Kungarra Formation.||||||07-APR-09
27276|Meteorite Bore Member|41957|6|Mentioned|p79|||||||||
27276|Meteorite Bore Member|43262|5|Briefly described|Map Legend||Proterozoic|of Kungarra Formation.||||||
27276|Meteorite Bore Member|43290|4|Described|p7||Proterozoic|Of Kungarra Formation.||||||23-MAR-09
27276|Meteorite Bore Member|44152|5|Briefly described|p188 Fig.2-161, p189|||300m thick. Volcanic boulders sourced from Woongarra Volcanics. Some clasts exhibit glacial striations or grooving.||Kungarra Formation.|||Mixtite or diamictite: abundant boulders (to 0.3m across) of sandstone and acid volcanics lie scattered in a matrix of greenish-grey siltstone.|
27276|Meteorite Bore Member|60373|6|Mentioned|p145 Tb. 1|||Of Turee Creek Group.||||||23-JUN-09
27276|Meteorite Bore Member|61276|5|Briefly described|p579|Siderian|Siderian|Within Turee Group, in Hardey syncline. Intruded by mafic sill with SHRIMP Pb/Pb baddelyite age of 2208 +/-10 Ma.||||||
27276|Meteorite Bore Member|62129|3|Fully described|p11|Archaean|Archaean|Of Kungarra Formation. Geological Province: Hamersley Basin. Pebble to cobble argillite and sandstone unit.||||||07-FEB-11
27276|Meteorite Bore Member|62130|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Kangarra Formation. Geological Province: Hamersley Basin, Pilbara Craton. Metadidmictite; clasts comprise metamorphosed felsic volcanic rock, chert, and sandstone.||||||
27276|Meteorite Bore Member|64384|5|Briefly described|p37, p40|||Of the Kungarra Formation (Turee Group). Mixtite of possible glacial origin.||||||07-FEB-11
27276|Meteorite Bore Member|66574|5|Briefly described|p914 Fig.3|||Unit in Kungarra Formation (Turee Creek Group). Glacigenic diamictite and siltstone.||||||15-SEP-14
27276|Meteorite Bore Member|67130|5|Briefly described|p3 fig 2, p6, p31, p41|Siderian|Siderian|Up to 270m thick. Age is maximum depositional age.|c. 2420|Kungarra Formation||Overlies Boolgeeda Iron Formation, overlain by Koolbye Formation, Kazput Formation, Beasley River Quartzite|Glacial diamictite, fine sandstone, siltstone and shale. Clasts up to 80cm in diameter, consisting primarily of porphyritic rhyolite with clasts of sandstone, chloritic siltstone, leucogabbro, chert and banded iron formation also present.|
27276|Meteorite Bore Member|68035|4|Described|p292, 294, Fig 6|Paleoproterozoic|Paleoproterozoic|Turee Creek Basin. Glacial diamictites up to 270 m thick at the type locality. Detrital zircon dating indicates a maximum depositional age of c. 2.42 Ga (Takehara et al., 2010).|Max age 2420 Ma. Min age >2210 Ma.|Of Kungarra Formation.||Overlain by Koolbye Formation.|Diamictite, fine-grained sandstone and shale at type locality.|
27276|Meteorite Bore Member|68280|5|Briefly described|p5, p44, p48, p57|Paleoproterozoic|Paleoproterozoic|||Kungarra Formation||Overlain by Koolbye Formation|Glacial diamictite, fine grained sandstones and siltstones, scattered throughout with pebble to boulder sized, subrounded to subangular clasts of porphyritic rhyolite.|
27276|Meteorite Bore Member|69003|5|Briefly described|p7-9|||||Kungarra Formation.|||Foliated siltstone. Contains dropstones.|
27276|Meteorite Bore Member|69543|5|Briefly described|p86-88, 92, 94|||Sulfur four-isotope ratios tabulated, discussed.|2.4 Ga.|Turee Creek Group.|||Glaciogenic mudstone and sandstone. Contains abundant detrital quartz and pyrite grains.|
27276|Meteorite Bore Member|69565|5|Briefly described|p131-132, p133 Fig.1, p140|||Hardey Syncline. Previously, erroneously correlated with Boolgeeda Iron Formation.|c.2420 Ma (MDA: Takehara et al., 2010).|Kungarra Formation.|||Contains diamictites with striated clasts.|
27276|Meteorite Bore Member|69754|4|Described|p315-p317, p321, p324, |Rhyacian|Rhyacian|Pilbara Craton. Glacial-marine deposit. Minimum age is derived from a Pb-Pb baddelyite date of an intruding dolerite sill interpreted as coeval with the Cheela Springs Basalt. A maximum depositional age is derived from detrital zircon dates of ca. 2420 Ma. Outcrops on the northern limb of the Hardey Syncline. See also p329-p330, p332, p337-p341.|2208 +/- 15 Ma (Muller et al, min age)|Kungarra Formation|||Glacial diamictites.|
27276|Meteorite Bore Member|70086|5|Briefly described|p195-196,202|Paleoproterozoic|Paleoproterozoic|Geological province: Pilbara Craton. Of the Hamersley Basin. Glaciogenic, marine. Minimum age of Kungarra Formation constrained by U-Pb ages of detrital zircons in the Meteorite Bore Member (Takehara et al., 2010). Records mass independent sulfur isotope fractionation (Williford et al., 2011), a proxy for the near-absence of environmental oxygen (Farquhar et al., 2000); indicating the lower part of Meteorite Bore Member was deposited during the final stages of the Great Oxidation Event (GOE).||Unit of Kungarra Formation.||Underlain by Kungarra Formation, and locally by Boolgeda Iron Formation.||
27276|Meteorite Bore Member|70958|4|Described|p2|Paleoproterozoic|Paleoproterozoic|||of Kungarra Formation||Includes erratics resembling Woongarra Dacite and underlying BIF.|Diamictite, erratics including BIF and acid igneous rocks.|
27276|Meteorite Bore Member|71112|5|Briefly described|p71-73,78|||Geological province: Pilbara Craton. Evidence of glacial affinities; diamictites interpreted as debrites i.e. subaequeous debris-flow deposits.||Unit of Kungarra Formation.|||Diamictites, sandstones and associated mudrocks.|
27276|Meteorite Bore Member|71550|4|Described|p34-38,41-42,44-47|Siderian|Siderian|Geological province: Of Hamersley Basin. Abbreviated MBM in text. Detrital zircons yielding maximum depositional age of c. 2420 Ma (Takehara et al., 2010). However, zircon analysis from this study indicate maximum depositional age of 2340+\-22 Ma, suggesting glaciation must be younger than that.  Phillepot et al., 2007 reported Re-Os isochron age fo 2310+\-7 Ma from authigenic pyrite in the MBM.||Unit of Kungarra Formation.||||03-SEP-19
27276|Meteorite Bore Member|72570|6|Mentioned|p2|||Represents a glacio-eustatic cycle alongside another younger and tinner unit of coarse glacial diamictite (unnamed).||Kungarra Formation||||
27276|Meteorite Bore Member|72712|5|Briefly described|p6, p14, p17-19, p30, p42-p44, p46-49.|Rhyacian|Siderian|The type section is on the northern limb of the Hardey Syncline in the vicinity of the TCDP2 drillhole. A 'type area near meteorite Bore on the southern limb of the syncline' is also discussed [?]. Thickness variable. At least 438-270m. SHRIMP U-Pb baddeleyite crysallisation age determined by Müller et al. (2005). Maximum depositional ages from SHRIMP U-Pb detrital zircon studies suggest Woongarra Rhyolite and older units were the main source rock. Depositional age c.<2340 Ma. Diamictites were correlated with this member as they are viewed as a distictive chronostratigraphic marker. This member is the lower one of two glaciogenic horizons, the Calgra Member member being the uppermost. See also p55, p57, p9, p18, p35, p36 Fig.25, p51.|2312.7 +/- 23 Ma diagenetic Re-Os isochron age.|Kungarra Formation||In fault contact with (younger) Anthiby Formation?|Diamictites interbedded with thin mudstone and fine-grained sandstone intervals. Diamictite clasts are faceted and striated in outcrop, and include a wide variety of compositions.|
27276|Meteorite Bore Member|73538|5|Briefly described|p2 Fig. 1B, p3-4|Siderian|Siderian|Yielded a Re-Os age of 2313 +/- 6 Ma from diagenetic pyrite (Philippot et al., 2018).|2313 +/- 6 Ma Re-Os|Kungarra Formation|||Glacial diamictite.|
68497|Miaree Granite|63441|2|Defined|p10 Tb. 2|Archean|Archean|Of the Maitland River Supersuite. Intrudes Roebourne Group, the Regal Formation and Cleaverville Formation. Age: 2997+/-3Ma. Geological province: Pilbara Craton.||||||07-FEB-11
68497|Miaree Granite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Maitland River Supersuite. Geological province: Pilbara Craton.  Monzogranite and syenogranite; foliated; metamorphosed.||||||07-NOV-08
68497|Miaree Granite|64580|4|Described|map legend||Mesoarchean|Of Maitland River Supersuite. Monzogranite and syenogranite; foliated metamorphosed.||||||15-DEC-08
68497|Miaree Granite|67201|5|Briefly described|p16-17 Fig.9|Archean|Archean|Pilbara Craton. In Roebourne-Karratha area.||Maitland River Supersuite|||Monzogranite and syenogranite; foliated; metamorphosed.|24-NOV-16
68497|Miaree Granite|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Maitland River Supersuite.|||Monzogranite and syenogranite; foliated metamorphosed|
68497|Miaree Granite|70775|5|Briefly described|p15-p16, p24 tbl 3, p53|||Pilbara Craton. Age derived from Nelson., 1998e. Together with the Erramurra Monzogranite and the Hearson Cove Monzogranite forms the Dampier Granitic Complex. This unit outcrops sporadically along the southeast shores of salt evaporation ponds between the Maitland River and Karratha Airport. Relatively homogenous monzogranite of this intrusion has been dated at 2997 +/- 3 Ma (Nelson, 1998e).|c. 3255 Ma (Pb/Pb zircon age)|Maitland River Supersuite|||Monzogranite and syenogranite; foliated and metamorphosed.|
68497|Miaree Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, syenogranite|
68497|Miaree Granite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|De Grey Superbasin.|2997+/-3 Ma.|Maitland River Supersuite|||Monzogranite and syenogranite; foliated; metamorphosed.|
75925|Middle Spring Granite|66105|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Moorarie Supersuite. Pale grey, gneissic to foliated metamonzogranite; derived from medium-grained equigranular to sparsely porphyritic biotite monzogranite. Includes an unnamed unit of pale grey, recrystallised mylonitic metamonzogranite.||||||
75925|Middle Spring Granite|66110|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Moorarie Supersuite. Pale grey, gneissic to foliated metamonzogranite; derived from a medium-grained equigranular to sparsely porphyritic biotite monzogranite.||||||
75925|Middle Spring Granite|66299|4|Described|p13, p136, pp173-176.|Paleoproterozoic|Paleoproterozoic|Strongly deformed to mylonitized granites. Tectonically interleaved with lenses of Leake Spring Metamorphics. Contains rafts of Halfway Gneiss.|1788 +/- 7 Ma.|Unit in Moorarie Supersuite.||Intruded by Rubberoid Granite, and granites of Durlacher Supersuite. Is faulted against Leake Spring Metamorphics. Is overlain unconformably by Edmund Group.|Pale grey, gneissic to foliated metamonzogranite; derived from a medium-grained equigranular to sparsely porphyritic biotite monzogranite.|
75925|Middle Spring Granite|67843|6|Mentioned|p2 Fig.1. |Paleoproterozoic|Paleoproterozoic|||||||
75925|Middle Spring Granite|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|||Moorarie Supersuite|||Pale grey, recrystallized mylonitic metamonzogranite and gneissic to foliated metamonzogranite; derived from medium-grained equigranular to sparsely porphyritic biotite monzogranite|
75925|Middle Spring Granite|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|100k_interpgeop_lut.csv|1788 Ma||||Gneissic to foliated and recrystallized mylonitic metamonzogranites derived from medium grained, equigranular to sparsely porphyritic biotite monzogranite.|
75925|Middle Spring Granite|70814|6|Mentioned|p65|||||||||
75925|Middle Spring Granite|71869|5|Briefly described|p6, app p10|||Capricorn Orogen.|1788 +/- 7 Ma (igneous cryst. Age)|Moorarie Supersuite|||Gneissic metamonzogranite.|
73383|Midgengadgi Monzogranite|63417|5|Briefly described|Map legend|Archean|Archean|Of the Cleland Supersuite. Geological Province: Pilbara Craton. Biotite monzogranite; seriate to porphyritic; medium- to coarse-grained, weakly metamorphosed.||||||07-NOV-08
73383|Midgengadgi Monzogranite|65829|2|Defined|p7 Fig.3, p32, p43.|Paleoarchean|Paleoarchean|New name. Named after Midgengadge (sic) Creek, a tributary of Oakover River. A small intrusion of unknown shape, 2 km by 2 km, on southeast margin of the exposed Yilgalong Granitic Complex. Type areas are well-exposed tor-covered sheets 17.5 km southeast of Dingo Well. Lack of deformation implies no significant post-3274 Ma deformation event in this eastern side of the Yilgalong Granitic Complex.|3274 +/- 5 Ma (Bordokos et al. 2006a).|Unit in Cleland Supersuite.||Intrudes Elsie Creek Tonalite. Is overlain unconformably by the Kylena Formation.|Nonfoliated, seriate to porphyritic, medium- to coarse-grained leucocratic biotite monzogranite.|
80124|Mikado Gabbro|71212|4|Described|intro p2, p59, p46, p52, p53,|||Yilgarn Craton. One of 5 informal units that are together equivalent to the formal Bounty Igneous Complex. Outcrop characteristics discussed. Up to 250m thick. See also p89, p106, p108,  p213, p219.||||Intrudes the Never Can Tell Basalt. Overlies the Breakaways layered mafic-ultramafic complex. Overlain by the Wildcat Gabbro.|Medium to coarse-grained and mostly massive gabbro.|26-SEP-17
30319|Milba Formation|23621|2|Defined|p54 Appendix|Orosirian|Orosirian|See also page 18, 11 table 1. Age: ~1835 Ma. Previously mapped as part of Olympio Formation. Underlain by Olympio Formation. Geological Province: Halls Creek Orogen. Max. thickness: >1000 m.||||||14-NOV-06
30319|Milba Formation|23622|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
30319|Milba Formation|24173|4|Described|p19, p13 Tb.2|Paleoproterozoic|Paleoproterozoic|Geol.Prov: Halls Creek Orogen. Max Thickness: >1000m. Originally mapped as Olympio Fm. by Gemuts & Smith (1968). Age: >1843Ma. Possible correlative of Koongie Park Formation; or of Marboo Fm. and Tickalara Metamorphics in McINTOSH (Tyler et al 1997a).||||||07-NOV-08
30319|Milba Formation|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Metamorphosed (low grade) interlayered mudstone, siltstone, sandstone, carbonate, calc-silicate rock and basaltic volcanic and volcaniclastic rocks.||||||07-NOV-08
30319|Milba Formation|43854|5|Briefly described|Map Legend||Proterozoic|||||||
30319|Milba Formation|44868|5|Briefly described|Map Legend||Proterozoic|||||||
30319|Milba Formation|63866|5|Briefly described|p131|||There are no known isotopic dates for this unit.||||(presumably) Overlain by the Tickalara Metamorphics.|Tightly folded low-grade mudstone, siltstones, sandstones, carbonates and basaltic volcanics.|
30319|Milba Formation|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Metamorphosed (low-grade) interlayered mudstone, siltstone, sandstone, carbonate, calc-silicate rock, and basaltic volcanic and volcaniclastic rocks.||||||15-DEC-08
30319|Milba Formation|69099|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Metamorphosed (low-grade) interlayered mudstone, siltstone, sandstone, carbonate, calc-silicate rock, and basaltic volcanic and volcaniclastic rock.|03-AUG-15
30319|Milba Formation|69165|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Metamorphosed interlayered mudstone, siltstone, sandstone carbonate, calc-silicate and basaltic volcanic and volcaniclastic rock.|
30319|Milba Formation|69634|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Metamorphosed (low-grade) interlayered mudstone, siltstone, sandstone, carbonate, calc-silicate rock, and basaltic volcanic and volcaniclastic rock|
30319|Milba Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Turbiditic greywacke, siltstone and mudstone; lithic, feldspathic and quartz sandstone; calcareous rocks; chert; and minor mafic lavas and sills. Regionally metamorphosed to mainly greenschist facies; commonly strongly foliated|
30319|Milba Formation|73089|6|Mentioned|p33|Orosirian|Orosirian|Lamboo Province, Central Zone. Dominantly Paleoproterozoic detritus.|c. 1875-1855 Ma||||Includes metasedimentary units.|
31769|Milga Gneiss|23569|4|Described|p5 Tb. 1|Archean|Archean|Of the Narryer Terrane.   Granodioritic gneiss||||||07-NOV-08
31769|Milga Gneiss|23574|5|Briefly described|Map Legend|Archean|Archean|Underlying unit Dugel Gneiss.||||||07-NOV-08
31769|Milga Gneiss|23576|5|Briefly described|Map Legend|Archean|Archean|Underlying unit Dugel Gneiss.||||||07-NOV-08
31769|Milga Gneiss|23577|5|Briefly described|Map Legend|Archean|Archean|Underlying unit Dugel Gneiss.||||||07-NOV-08
31769|Milga Gneiss|24114|5|Briefly described|p5 Fig.4|Archean|Archean|Geological Province: Yilgarn Craton. Age: c. 3000 Ma||||||07-NOV-08
31769|Milga Gneiss|43835|5|Briefly described|Map Legend|Archean|Archean|Age about 3000Ma.||||||07-NOV-08
31769|Milga Gneiss|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||felsic gneiss|
31769|Milga Gneiss|73526|5|Briefly described|p2 Fig.1, p3|||Narryer Terrane. Derived from a granodioritic precursor emplaced at 2994+/-6 Ma. See also Milga gneiss p4 Tb.1.|||||Gneissic rocks.|
26030|Millajiddee Member|22741|5|Briefly described|P25, Table3 P14||Sakmarian|||||||
26030|Millajiddee Member|22767|5|Briefly described|Table3 P16, P21||Early Permian|||||||
26030|Millajiddee Member|22776|4|Described|Table.3|Early Permian|Early Permian|Parent: Carolyn Formation.||||||17-NOV-08
26030|Millajiddee Member|30338|2|Defined|p101|Sakmarian|Sakmarian|||||||
26030|Millajiddee Member|30342|6|Mentioned|p103|||||||||
26030|Millajiddee Member|36224|5|Briefly described|Map legend|Early Permian|Early Permian|Of the Grant Group.  Sandstone, minor mudstone.||||||01-FEB-05
26030|Millajiddee Member|36225|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26030|Millajiddee Member|36634|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26030|Millajiddee Member|37914|5|Briefly described|p449|||||||||08-FEB-10
26030|Millajiddee Member|38217|5|Briefly described|p269|||||||||
26030|Millajiddee Member|41315|6|Mentioned|p149|||||||||
26030|Millajiddee Member|41839|5|Briefly described|p27|||||||||
26030|Millajiddee Member|42392|6|Mentioned|p120|||Member of Carolyn Formation||||||
26030|Millajiddee Member|42613|5|Briefly described|P 10, Table 1, Fig.3|||||||||
26030|Millajiddee Member|64643|4|Described|p8, p21|Sakmarian|Sakmarian|Of Carolyn Formation. Well exposed sandstone, 30m thick. Overlies Wye Worry Member.||||||
26030|Millajiddee Member|66949|4|Described|p10-14, p16, p18-20, p57 Appx.3|Sakmarian|Sakmarian|See also p78,81 Appx.5. Type section detailed. Up to 70m thick; fluvial to tidally influenced deposits. Contains trace fossils. Resembles Clianthus Formation.||Upper unit in Carolyn Formation.||Conformably overlies Wye Worry Member.|Massive and cross-bedded medium- to coarse-grained sandstone.|02-NOV-15
26030|Millajiddee Member|72497|5|Briefly described|p1, p4-5, 7, p9-12, 19-20, 26-27-29.|Sakmarian|Sakmarian|Described as being within the Western St George ranges. Shallow-water marine platform/subtidal environment to deltaic sediments deposited within a channel environment.||Carolyn Formation||Shown as overlying Wye Worry Member. Unconformably underlies Poole Sandstone and Nura Nura Member.|Includes siltstone, claystone, horizontally laminated sandstone and massive sandstone with dropstones.|
26030|Millajiddee Member|73117|5|Briefly described|p23, p117|||Of Crowe and Towner (1975). Known from outcrop; not readily identified in the subsurface. Given that the authors consider the parent unit to be informal, they provisionally regard this subdivision as a local formation within the Grant Group.||Carolyn Formation, Grant Group||Underlain by Wye Worry Member. Overlain by Poole Sandstone.|Massive and cross-bedded sandstone.|
35510|Millars Monzogranite|23787|5|Briefly described|p32|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
35510|Millars Monzogranite|24167|4|Described|p27, p7 Fig.3, p31 Fig 20|||Geological Province: Yilgarn Craton||||||
35510|Millars Monzogranite|24245|6|Mentioned|p7 Tb. 1|Archean|Archean|Porphyritic granite.  Age: c.2635.  Geological Province: Yilgarn Craton.||||||07-NOV-08
35510|Millars Monzogranite|24335|5|Briefly described|Map legend|Archean|Archean|Age: c.2711Ma.  Geological Province: Yilgarn Craton||||||07-NOV-08
35510|Millars Monzogranite|70156|4|Described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Youanmi Terrane events (3200-2600 Ma).|2654-2600 Ma (inferred)||||Quartz-rich monzogranite|
35510|Millars Monzogranite|70794|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean||2654-2600 Ma inferred||||Quartz rich monzogranite.|
35510|Millars Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
35510|Millars Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||||||Quartz-rich monzogranite.|
33454|Millindinna Intrusion|23793|5|Briefly described|p28|||Informal||||||
33454|Millindinna Intrusion|44863|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
33454|Millindinna Intrusion|63372|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Mallina Basin and east Pilbara. Undivided mafic and ultramafic rocks as layered sills; metamorphosed.||||||07-NOV-08
33454|Millindinna Intrusion|63441|5|Briefly described|p12 tb. 2, p38|Archean|Archean|Supersedes Millindinnah Complex - incorrectly spelt in this publication - should be Millindinna.||||||07-FEB-11
33454|Millindinna Intrusion|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton. Also appears as Millindinnah Intrusion.||Of the Sisters Supersuite.|||Comprises gabbro, pyroxenite, and peridotite; metamorphosed.|30-APR-14
33454|Millindinna Intrusion|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Sisters Supersuite|||Gabbro, pyroxenite, and peridotite; metamorphosed. Schistose metagabbro,  serpentinite, serpentine-tremolite and serpentine-chlorite schist, serpentinized peridotite. Interleaved schist and banded iron-formation, chert and local cordierite hornfels.|
33454|Millindinna Intrusion|69300|5|Briefly described|map legend|Archean|Archean|Mallina Basin||Pilbara Supergroup|||undivided gabbro, mafic, and ultramafic rocks forming layered sills; metamorphosed|
33454|Millindinna Intrusion|70775|6|Mentioned|p65|||||||||
33454|Millindinna Intrusion|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||mafic and ultramafic rock|
33454|Millindinna Intrusion|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mallina Basin, De Grey Superbasin.||Langenbeck Suite|||Gabbro, pyroxenite, and peridotite; metamorphosed.|
39039|Milliwindi Dolerite|24122|5|Briefly described|p12|Cambrian|Cambrian|Age: 513+/-12Ma (SHRIMP).||||||
39039|Milliwindi Dolerite|24297|5|Briefly described|p18|Middle Cambrian|Middle Cambrian|Dolerite dyke.  Age: 513+/-12Ma (SHRIMP zircon,  Hanley and Wingate, 2000).||||||
39039|Milliwindi Dolerite|24303|6|Mentioned|p62 Appendix|||Age: 513 +/- 12 Ma. Correlates with Antrim Plateau Volcanics.||||||
39039|Milliwindi Dolerite|60685|6|Mentioned|p18|Early Cambrian|Early Cambrian|Dolerite dyke in west Kimberley region. Age: 513 +/- 12Ma (SHRIMP Zircon, Hanley and Wingate, 2000).||||||24-NOV-09
39039|Milliwindi Dolerite|64589|5|Briefly described|dated_samples file||Cambrian|U-Pb zircon crystallization age 513 +/-12 Ma. Kimberley.||||||12-NOV-08
39039|Milliwindi Dolerite|66526|6|Mentioned|p7, p17, p27.|||In Hanley and Wingate, (2000). Referred to on p17 and p27 as Milliwindi dolerite dyke. Kimberley Province; coeval and geochemically comagmatic with the Kalkarindji Large Igneous Province lavas.||||||
39039|Milliwindi Dolerite|69445|5|Briefly described|p30:1, 6, 10, 16-17|Cambrian|Cambrian|Hanley and Wingate (2000). A 250km long feeder dyke for the Antrim Plateau Volcanics (Kalkarindji Suite). SHRIMP U-Pb zircon age.|513 +/- 12 Ma (Hanley and Wingate, 2000).|Kalkarindji Suite.||||12-JUL-16
39039|Milliwindi Dolerite|69634|4|Described|GEOL_LUT_CSV files|Series 2|Series 2|Of Kalkarindji Large Igneous Province. Events: Alice Springs Orogeny. See 250k_interpgeol_lut.csv, 250k_geologyl_lut.csv.|510 Ma Isisotopic)|Unit of Kalkarindji Supersuite.|||Dolerite dyke|
39039|Milliwindi Dolerite|69660|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Kalkarindji Large Igneous Province.|c.510 Ma.||||Dolerite dyke.|
39039|Milliwindi Dolerite|70126|5|Briefly described|Map legend|Cambrian|Cambrian|Kalkarindji Large Igneous Province.|c.510 Ma.||||Dolerite dykes.|
39039|Milliwindi Dolerite|70154|6|Mentioned|100k_geologyp_lut.csv|Cambrian||See also 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv.|510 +/-1Ma|Kalkarindji Supersuite |||Dolerite dyke.|22-SEP-17
39039|Milliwindi Dolerite|70826|6|Mentioned|p14 tbl 5|Cambrian|Cambrian|West Kimberley.|512 Ma|||||
39039|Milliwindi Dolerite|71267|4|Described|GEOL_LUT_CSV files|Series 2|Series 2|Of the Kalkarindji LIP. Events: Alice Springs Orogeny (450-295 Ma). See 100k_interpgeop_lut.csv, 100k_geologyp_lut.csv, 250k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 1m_interpgeol_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv, 100k_geologyl_lut.csv.|510+\-1 Ma (isotopic)|Unit of Kalkarindji Supersuite.|||Dolerite dyke|
73464|Millstream Formation|63372|5|Briefly described|Map Legend|Pleistocene|Miocene|Dolomite and calcareous dolomite, with silcrete, clay, and local basal conglomerate.||||||
73464|Millstream Formation|64654|5|Briefly described|Map Legend|Neogene|Paleogene|Dolomite, calcareous dolomite, and calcrete; minor clay and basal conglomerate; local residual silcrete and chert breccia.||||||
73464|Millstream Formation|64657|5|Briefly described|Map Legend|Neogene|Paleogene|Dolomite, calcareous dolomite, and calcrete; minor clay and basal conglomerate; local residual silcrete and chert breccia.||||||
73464|Millstream Formation|65724|6|Mentioned|map legend|||Mentioned in description of unnamed alluvial or lacustrine calcrete unit: probably includes units of similar ages to Oakover and Millstream Formations. ||||||
73464|Millstream Formation|69167|4|Described|geologyp_lut.csv|Neogene|Neogene||||||Dolostone and calcrete, and minor clay; local basal conglomerate; local residual silcrete and chert breccia.|
73464|Millstream Formation|69538|5|Briefly described|p527, p560|Holocene|Miocene|Fortescue Valley. Similar age to Oakover Formation. Overlies the CzD2 channel iron deposits. Age range from fresh-brackish and brackish water gastropods. Appears as Millstream Dolomite on p560.||||||
73464|Millstream Formation|69590|4|Described|100k_geologyp_lut.csv|Neogene|Neogene||23-2.59 Ma (inferred)||||Dolostone and calcrete, and minor clay; local basal conglomerate; local residual silcrete and chert breccia|
73464|Millstream Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolostone, calcrete, silcrete, clay|
37495|Millury Formation|50195|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Scorpion Group (Bangemall Supergroup).  Geological Province: Scorpion Basin.||||||23-JUN-04
37495|Millury Formation|64580|4|Described|map legend||Mesoproterozoic|Of Scorpion Group. Quartz sandstone; minor siltstone, local evaporite pseudomorphs.||||||15-DEC-08
37495|Millury Formation|64772|5|Briefly described|p13, Plate 1  legend|Proterozoic|Proterozoic|Of the Scorpion Group. Quartz sandstone, minor siltstone, local evaporite pseudomorphs.||||||01-MAR-11
37495|Millury Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone, conglomerate|
37495|Millury Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Paleoproterozoic|Scorpion Basin.||Scorpion Group|||Quartz sandstone; minor siltstone, local evaporite pseudomorphs.|
27196|Millyit Sandstone|7433|5|Briefly described|pp39-40, p52.|Early Triassic|Early Triassic|Gregory and southeast Fitzroy Sub-basins, Canning Basin. Fluvial deposits. Excellent aquifer potential and ideal hydrocarbon reservoir rock, confined or capped by Blina Shale.|||||Medium- to coarse-grained quartzose sandstone with large crossbedding, overlying thinner units of finer sandstone and intraformational clay-clast conglomerate.|
27196|Millyit Sandstone|13354|6|Mentioned|p376 Fig.7.|Late Permian|Late Permian|Onshore Canning Basin. Unconformably overlies Liveringa Group and underlies Blina Shale.||89||||28-OCT-14
27196|Millyit Sandstone|22741|5|Briefly described|p29, Table3 P11||Triassic|||||||10-FEB-20
27196|Millyit Sandstone|22764|4|Described|Table2,p9||Early Triassic|50 m. Disconformable on Condren Sandstone, slightly disconformable beneath Blina Shale.||||||10-FEB-20
27196|Millyit Sandstone|22767|5|Briefly described|Table3 p14, p22||Early Triassic|||||||10-FEB-20
27196|Millyit Sandstone|33518|4|Described|Table 1|||||||||
27196|Millyit Sandstone|33519|6|Mentioned|Map legend|Triassic|Triassic|||||||
27196|Millyit Sandstone|35120|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
27196|Millyit Sandstone|35124|6|Mentioned|Map legend|Early Triassic|Early Triassic|Prob.Early Triassic||||||
27196|Millyit Sandstone|35205|6|Mentioned|Map legend|Triassic|Triassic|||||||
27196|Millyit Sandstone|36225|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
27196|Millyit Sandstone|36257|6|Mentioned|Table 2.1|||||||||
27196|Millyit Sandstone|36634|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
27196|Millyit Sandstone|36890|4|Described|p348|||||||||
27196|Millyit Sandstone|38878|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
27196|Millyit Sandstone|41158|6|Mentioned|Plate 3|||||||||
27196|Millyit Sandstone|41169|6|Mentioned|p148|||||||||
27196|Millyit Sandstone|43563|6|Mentioned|Fig.9,p15|Early Triassic|Late Permian|||||||
27196|Millyit Sandstone|43666|6|Mentioned|p45,Table 2||Scythian|||||||
27196|Millyit Sandstone|43932|4|Described|p10,Tb.1 p5|Triassic|Permian|||||||
27196|Millyit Sandstone|44143|4|Described|p434 Table 4-19, p447, p448 Fig.4-106|Triassic|Triassic|Up to 90m thick; medium to fine sandstone, fluvial. Unconformably overlies Hardman Formation; disconformably overlies Condren Sandstone. Type section: head of Spring Creek (CROSSLAND: 19deg 12' S, 125deg 33' 30" E). Fossil plants.||||||23-NOV-17
27196|Millyit Sandstone|44998|2|Defined|p145||Jurassic|Overlies Liveringa Formation. On many pages. p.133-6,143,185,map.||||||
27196|Millyit Sandstone|45153|2|Defined|App.5-85|Early Triassic|Late Permian|Late Permian to Early Triassic. Type section: At the head of Spring Creek, Milllyit Range (19degrees 12 '00 "S, 125degrees35 '30"E).  Lithology: In BMR Lucas No. 13 - siltstone: grey and black, carbonaceous with thin- bedded fine-grained sandstone near the base; overlain by sandstone: clear, white, massive, medium to coarse-grained, quartzose, high-angle cross-bedding, quartz pebbles. The transitional unit with the Blina Shale consists of sandstone: fine to medium-grained, quartzose, in medium to cross-bedded sets up to 30 cm thick; and interbedded siltstone; carbonaceous and micaceous. In outcrop the medium to coarse-grained sandstone predominates, probably because the softer siltstones have been eroded. Cyclic sedimentation (5m thick cycles) and fining-upwards sequences are known in outcrop.||||||15-DEC-22
27196|Millyit Sandstone|45158|3|Fully described|p18|||||||||
27196|Millyit Sandstone|46863|6|Mentioned|p25|||||||||
27196|Millyit Sandstone|46912|6|Mentioned|Table 1|||Analytical data of Canning Basin cores||||||
27196|Millyit Sandstone|63929|6|Mentioned|p131 Fig.2.|Early Triassic|Early Triassic|Onshore Canning Basin.||||Is overlain by Blina Shale.||
27196|Millyit Sandstone|64580|4|Described|map legend||Early Triassic|Fine- to coarse-grained sandstone; minor conglomerate. Eastern Canning Basin.||||||09-DEC-08
27196|Millyit Sandstone|64643|5|Briefly described|p9, p3 Fig. 2|Lopingian|Lopingian|Up to 90m of medium to fine-grained sandstone.||||||24-NOV-08
27196|Millyit Sandstone|65301|5|Briefly described|p5 Fig. 4|Late Permian|Late Permian|Geological province: Canning Basin.||||||
27196|Millyit Sandstone|65449|6|Mentioned|p6|Early Triassic|Lopingian|||||Unconformably overlies Liveringa Group. Is overlain by Blina Shale.||
27196|Millyit Sandstone|66124|5|Briefly described|p169, p170 Fig.2|Induan|Induan|Canning Basin. Fluvial, maximum 90m thick. Grades NW into Blina Shale; underlies Blina Shale.||||||
27196|Millyit Sandstone|66949|4|Described|p26-27, p46 Appx.2, p55 Appx.3|Early Triassic|Early Triassic|See also p60 Appx.4; p76,78 Appx.5. Elliot, in McWhae et al. (1958). Type section detailed. Up to 93m thick (in BMR Lucas 13); fluvial deposits. Biostratigraphic zonation. Available core detailed.||||Overlies Godfrey beds; also Hardman Formation unconformably, and Condren Sandstone disconformably. Interfingers with and is overlain conformably by Blina Shale.|Medium- to fine-grained sandstone.|04-NOV-15
27196|Millyit Sandstone|68007|6|Mentioned|p4|Late Permian|Late Permian|Canning Basin.||||||25-FEB-20
27196|Millyit Sandstone|68656|5|Briefly described|GEOL_LUT_CSV/500k_geologyp08_lut||Early Triassic||||||Fine- to coarse-grained sandstone; minor conglomerate.|
27196|Millyit Sandstone|68902|6|Mentioned|p9 fig 5|Permian|Permian|||||Unconformably overlies Liveringa Group, disconformably overlain by Blina Shale.||
27196|Millyit Sandstone|69099|5|Briefly described|500k_geologyp08_lut.csv||Early Triassic||||||Fine- to coarse-grained sandstone; minor conglomerate.|03-AUG-15
27196|Millyit Sandstone|69182|6|Mentioned|Ch4 p3, Ch4 p9, Ch4 p15-p16|Lopingian|Lopingian|Canning Basin. See also Ch4 p38, Ch4 p43-p45, Ch4 p47, Ch4 p50-p58, Ch4 p74-p77, Ch4 p88, Ch4 p90. ||||Unconformably overlies the Liveringa Group. Conformably overlain by the Blina Shale.||
27196|Millyit Sandstone|69587|5|Briefly described|500k_geologyp08_lut.csv||Early Triassic||||||Fine- to coarse-grained sandstone; minor conglomerate|
27196|Millyit Sandstone|70154|4|Described|500k_interpgeop14_lut.csv|Lower Triassic|Lower Triassic||247-252 Ma||||Fine to coarse grained sandstone; minor conglomerate|
27196|Millyit Sandstone|70774|5|Briefly described|p4, p9|Early Triassic|Lopingian|Fitzroy Trough and Lennard Shelf, Canning Basin.||||Overlies the Liveringa Group. Overlain by the Blina Shale.||10-FEB-20
27196|Millyit Sandstone|71146|5|Briefly described|p6|Lopingian|Lopingian|Canning Basin.||||Overlain by the Blina Shale.|Sandstone.|
27196|Millyit Sandstone|71267|4|Described|GEOL_LUT_CSV files|Early Triassic|Early Triassic|Of Canning Basin. Events: Point Moody Extension (300-242 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|252.17-247.2 Ma (inferred-biostrat)||||Poorly to thinly bedded and cross bedded and in places graded fluvial fine to medium grained sandstone with minor conglomerate and siltstone; partly fossiliferous with plant fossils and palynomorphs|
27196|Millyit Sandstone|71623|5|Briefly described|p345 fig 2|||Canning Basin. Hosts plant megafossils.||||Unconformably overlain by the Blina Shale.||
27196|Millyit Sandstone|71894|5|Briefly described|p4|Lopingian|Lopingian|Canning Basin.||||Disconformably overlies the Liveringa Group. Overlain by the Blina Shale.|Sandstone.|
27196|Millyit Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Early Triassic|Early Triassic|Canning Basin.  Age from biostratigraphy.|||||Fine- to coarse-grained sandstone; minor conglomerate.|
27196|Millyit Sandstone|72499|5|Briefly described|p7 Fig.6.|Early Triassic|Lopingian|Located in the Fitzroy Trough.||||Overlies Liveringa Group and underlies Blina Shale.||
27196|Millyit Sandstone|73117|5|Briefly described|p3, p123|Lopingian|Lopingian|Canning Basin.||||Disconformably underlain by Liveringa Group. Overlain by Blina Shale.|Dominantly sandstone.|
27196|Millyit Sandstone|73445|5|Briefly described|p3, 6, 8, 12-14, 24, 34, 36, 42-43|Triassic|Triassic|See also p65-118. Canning Basin. 90m thick. Whole-rock and regolith chemistries tabulated.||||Disconformably overlies Liveringa Group. Is overlain transitionally by Blina Shale.|Sandstone, siltstone and minor conglomerate.|
73397|Minara Group|65147|5|Briefly described|p3, p4 Fig.3, p5   |||Murrin Domain greenstones.|||Includes Murrin Murrin, Minerie, Welcome Well Formations.||Calc-alkaline-tholeiite-komatiite succession.|
73397|Minara Group|65180|4|Described|map legend|Neoarchean|Neoarchean|Metamorphosed volcanic rocks (mostly basic) and volcaniclastic sandstones. Of Yilgarn Craton. Includes Murrin Murrin Formation, Minerie Formation, Welcome Well Formation. Age from constituent units.||||||24-NOV-09
73397|Minara Group|69152|5|Briefly described|minerie_lut. files|||Murrin Domain, Kurnalpi Terrane, Yilgarn Craton|||Includes Murrin Murrin Formation, Minerie Formation, Welcome Well Formation.|||
73397|Minara Group|70153|5|Briefly described|Minerie_100k_geologyp_lut.csv|Archean|Archean||||Includes Minerie Formation, Murrin Murrin Formation, Welcome Well Formation|||
73397|Minara Group|71270|5|Briefly described|GEOL_LUT_CSV files||Archean|Geological province: Murrin Domain, Kurnalpi Terrane, Yilgarn Craton, West Australian Craton. See minerie_100k_geologyp_lut.csv, minerie_100k_geologyl_lut.csv, minerie_100k_interpgeop_lut.csv.|||Includes Minerie Fomation, Murrin Murrin Formation, Welcome Well Formation.|||
74850|Mindoolah Tonalite|64891|5|Briefly described|p50-51 Tb. 1|Archean|Archean|Of the Cullculli Suite (Annean Supersuite). Age: ?2750Ma. Geological province: Murchison Domain. Tonalite; metamorphosed. See also Mindoola Tonalite.||||||07-FEB-11
73394|Minerie Formation|65147|5|Briefly described|p5 Fig.6, p6, p12-13   |||||Unit in Minara Group.||Overlies Welcome Well Formation. Is overlain by Murrin Murrin Formation.|Gabbro, pillow basalt and hyaloclastite, felsic volcaniclastic and epiclastic rocks; basaltic piilow lava, autoclastic breccia facies. Flow interiors are commonly crystalline (doleritic to cumulate).|
73394|Minerie Formation|65180|5|Briefly described|map legend|Neoarchean|Neoarchean|Metamorphosed basalt, and some felsic volcaniclastic sandstone and chert. Of the Minara Group, Murrin Domain, Yilgarn Craton. Age inferred from that of overlying Murrin Murrin Formation (c. 2698 Ma) and underlying Welcome Well Formation (c. 2704 Ma).|Inferred to be between 2704 Ma and 2698 Ma|Of the Minara Group||||24-NOV-09
73394|Minerie Formation|69152|4|Described|minerie_lut. files||Archean|Murrin Domain, Kurnalpi Terrane, Yilgarn Craton||Minara Group|Includes 14 unnamed subunits.||Basalt; aphanitic, amygdaloidal, pillow, porphyritic, fine/coarse crystalline, or with volcaniclastic texture; agglomerate or hyaloclastite breccia; dacite; dacitic siltstone; sandstone; chert, banded chert; all metamorphosed.|06-AUG-15
73394|Minerie Formation|70153|5|Briefly described|Minerie_100k_geologyp_lut.csv|Archean|Archean|See also minerie_100k_interpgeop_lut. csv. Murrin Domain, Kurnalpi Terrane.||Minara Group|||Basalts: aphanatic, amygdaloidal, porphyritic or pyroxene-spinifex textured; pillow basaltic andesite, basaltic fragmental rock; dacite and dacitic siltstone; felsic epiclastic sandstone; chert and banded chert; locally jaspilitic and/or brecciated.|
73394|Minerie Formation|71270|5|Briefly described|GEOL_LUT_CSV files||Archean|Geological province: Murrin Domain, Kurnalpi Terrane, Yilgarn Craton, West Australian Craton. See minerie_100k_geologyp_lut.csv, minerie_100k_geologyl_lut.csv, minerie_100k_interpgeop_lut.csv.||Unit of Minara Group.|||Basalt: amygaloidal, aphanitic, pillowed, porphyritic, pyroxene spinifex-textured, common volcaniclastic texture, metamorphosed; pillowed basaltic andesite; dacite and dacitic siltstone: metamorphosed; felsic epiclastic sandstone; metamorphosed.|
81890|Minga Dolerite|73102|4|Described|p1, p3, p6-10, p12-20, p31|||Capricorn Orogen, western. [Named here?]. An areally restricted swarm of non-dated dolerite dykes. North-northwesterly trending in the westernmost part of the orogen. Previously thought to be related to sills of the Narimbunna Dolerite; although herein shown to be geochemically and petrogenetically distinct, and they are not spatially associated. Represents mantle-derived magmas, possibly with compositions resembling E-MORB that were more or less continuously contaminated through assimilation of crustal material during emplacement. Dykes are up to 70 m wide, with strike lengths up to 25 km; difficult to identify in aeromagnetic images because they typically parallel the regional structural architecture and magnetic grain. Samples failed to yield dateable minerals. [Article includes detailed petrographic description, whole rock major and trace element composition, Sm-Nd isotope composition].||||Intrudes Pooranoo Metamorphics, Moorarie Supersuite, Durlacher Supersuite.|Strongly altered, melanocratic dolerite of high-Fe tholeiitic affinity.|
38088|Mingah Member|23570|6|Mentioned|p237 App. 1|||Abbreviation of Mingah Tuff Member.||||||
38088|Mingah Member|24352|6|Mentioned|Map legend|Archean|Archean|Parent: Tumbiana Formation.  Age: >2717Ma.  Geological Province: Hamersley Basin||||||07-NOV-08
38088|Mingah Member|50381|5|Briefly described|Map Legend|Archean|Archean|Of Tumbiana Formation (Fortescue Group). Geological Province: Hamersley Basin, Pilbara Craton.||||||07-NOV-08
38088|Mingah Member|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Tumbiana Formation. Age: c. 2719Ma. Geological Province: Pilbara Craton. Pisolithic mafic tuff, and tuffaceous siltstone and sandstone; thin carbonate units.||||||07-FEB-11
38088|Mingah Member|64654|5|Briefly described|Map Legend|Archaean|Archaean|Of Tumbiana Formation. Age: 2727-2721Ma. Geological Province: Pilbara Craton (Hamersley Basin). Basaltic to andesitic volcanoclastic sandstone and siltstone, and local quartz sandstone, shale and thin lenticular stromatolitic carbonate units.||||||
38088|Mingah Member|64656|5|Briefly described|Map Legend|Archaean|Archaean|Of Tumbiana Formation. Geological Province: Hamersley Basin. Basaltic to andesitic volcaniclastic sandstone and siltstone.||||||26-NOV-08
38088|Mingah Member|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Tumbiana Formation. Age: 2727-2721Ma.  Geological Province: Hamersley Basin. Basaltic to andesitic volcaniclastic sandstone and siltstone, and local quartz sandstone, shale, and thin lenticular stromatolitic carbonate units; locally thick basalt flows.||||||
38088|Mingah Member|65008|4|Described|p23|Neoarchean|Neoarchean|Hamersley Basin. Geochronology by: D.R. Nelson, 2001, GSWA Record 2001/2, p.129-132, 140-148, 175-177.|ca. 2719 Ma|Of the Tumbiana Formation||Overlain by the Meentheena Member.|Consists of thin- to medium-bedded mafic tuff interbedded with tuffaceous sandstone and siltstone, and thin carbonate beds that are less than 1m thick.|14-MAY-14
38088|Mingah Member|65724|5|Briefly described|map legend|Neoarchaean|Neoarchaean|Of Tumbiana Formation. Basaltic to andestic volcaniclastic sandstone and siltstone, quartz sandstone, shale and stromatolitic carbonate units; basalt flows. Age: 2727-2721 Ma (geochron. T. S. Blake et al 2004). Geol. Prov: Hamersley Basin, Pilbara Craton.||||||
38088|Mingah Member|65726|5|Briefly described|Map legend|Archean|Archean|Hamersley Basin, Pilbara Craton.||Of Tumbiana Formation.||Overlies Kylena Formation.|Pisolitic tuff, and tuffaceous shale, siltstone and sandstone; minor basalt and thin carbonate units, locally stromatolitic.|
38088|Mingah Member|65727|5|Briefly described|Map legend|Neoarchean|Neoarchean|Fortescue Basin.||Of Tumbiana Formation.||Overlies Kylena Formation.|Basaltic to andesitic volcaniclastic sandstone and siltstone (common accretionary lapilli), quartz sandstone, shale, and thin lenticular stromatolitic carbonate units; locally thick basalt flows.|
38088|Mingah Member|65827|3|Fully described|p12 Tb.3, p33 Fig.6; p38-40|Neoarchean|Neoarchean|Of Tumbiana Formation (Fortescue Group); formerly Mingah Tuff Member (Lipple, 1975). 2727 +/- 5 Ma and 2721 +/- 4 Ma (Blake, 2001; Blake et al. 2004). Conformably underlies Meentheena Member; shown equivalent to part of Mount Jope Supersequence(1). Phreatomagmatic volcaniclastic/volcanigenic sedimentary rocks with tuff; minor basaltic lavas; intruded by thick dolerite sills.||||||
38088|Mingah Member|65829|4|Described|p10,p15,  p20, p22.|Neoarchean|Neoarchean|Formerly Mingah Tuff Member (Lipple 1975). Phreatomagmatic volcaniclastic and volcanogenic sedimentary rocks with minor basaltic lavas. Not well exposed. Intruded by thick dolerite sills and dykes.|c.2727 - 2721 Ma.|Basal unit in Tumbiana Formation.|||Basaltic to andesitic volcaniclastic grey-green sandstone and siltstone; accretionary lapilli interbeds common; local quartz sandstone, shale and thin lenticular stromatolitic carbonate units.|
38088|Mingah Member|66685|4|Described|p217-22, 230-236|Archean|Archean|Lipple (1975). 150m thick succession at Pelican Pool on the Nullagine River. Detailed description included. ||Tumbiana Formation||Conformably overlies Kylena Formation. Grades laterally into, and is overlain by, Meentheena Member.|Volcaniclastic dominated. Includes volcaniclastic sandstone (glass shards and accretionary lapilli), tuff (mafic>felsic), minor mudstone, limestone +/- stromatolites, and basalt. Diverse sedimentary structures.|
38088|Mingah Member|67201|5|Briefly described|p29 Fig.15|||In northern Pilbara Craton, Northern Fortescue Basin, Northeast Pilbara Sub-basin.||Tumbiana Formation||||
38088|Mingah Member|68056|5|Briefly described|p171-172, 175-181, 184-186, 188-191|Archean|Archean|Pilbara Craton. Alluvial fan deposits: upwards progression from lower shoreface to foreshore facies. Fe, C isotope data and pyrite shapes tabulated.||Basal Tumbiana Formation.||Is overlain by Meentheena Member.|Pebble- to cobble-sized conglomerate and intercalations of coarse-grained to very coarse-grained calcareous and tuffaceous sandstones; breccia; mudstone layers.|
38088|Mingah Member|68282|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.|2727-2715 Ma, age inferred from parent unit|Of the Tumbiana Formation|||Basaltic to andesitic volcaniclastic sandstone and siltstone (common accretionary lapilli), and local quartz sandstone, shale, and thin lenticular stromatolitic carbonate units; locally thick basalt flows.|12-JUN-14
38088|Mingah Member|69012|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.|2727-2715 Ma (Arndt et al 1991; Blake et al 2004)|Tumbiana Formation.|||Basaltic to andesitic volcaniclastic sandstone and siltstone (common accretionary lapilli), and local quartz sandstone, shale, and thin lenticular stromatolitic carbonate units; locally thick basalt flows.|26-OCT-15
38088|Mingah Member|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Tumbiana Formation|||Basaltic to andesitic volcaniclastic sandstone and siltstone (common accretionary lapilli), and local quartz sandstone, shale, and thin lenticular stromatolitic carbonate units; locally thick basalt flows|
38088|Mingah Member|69301|5|Briefly described|p18 Fig.7|||Pilbara Craton. Fortescue Basin. Northeast Pilbara Sub-basin, Sequence 2.||Tumbiana Formation||||
38088|Mingah Member|69411|5|Briefly described|p282,286,292|Neoarchean|Neoarchean|Geological province: Pilbara Craton. Interpeted as fluvial and shallow marine.||Unit of Tumbiana Formation.||Overlain by Meentheena Member.|Sandstones and subaerial lava flows with volcaniclastic and minor carbonate rocks.|05-JUL-19
38088|Mingah Member|69590|4|Described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Of Northeast Pilbara Sub-basin, Fortescue Basin. Events: Pilbara Craton breakup.|2727-2715 Ma (inferred)|Unit of Tumbiana Formation.|||Basaltic to andesitic volcaniclastic sandstone and siltstone (common accretionary lapilli), and local quartz sandstone, shale, and thin lenticular stromatolitic carbonate units; locally thick basalt flows|
75920|Minigwal Suite|66113|5|Briefly described|Map legend|Archean|Archean|Burtville Terrane, Yilgarn Craton. Age c.2769 to c.2765 Ma. Comprises Hope Campbell, Surprise, and Baseline Orthogneisses.||||||
75920|Minigwal Suite|68107|5|Briefly described|p611||||||Includes the Hope Campbell Orthogneiss and Surprise Orthogneiss.||Migmatitic orthogneiss.|
75920|Minigwal Suite|68186|5|Briefly described|Plate 1A|Archean|Archean|Burtville Terrane, Yilgarn Craton.|2769-2765 Ma (Fletcher et al., 2001).||||Granitic gneiss.|
75920|Minigwal Suite|69152|5|Briefly described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Burtville Terrane, Eastern Goldfields Superterrane, Yilgarn Craton|Granite protoliths ~2770 Ma||Includes Hope Campbell Orthogneiss, Baseline Orthogneiss, Surprise Orthogneiss.||Migmatitic quartz-biotite orthogneiss; migmatitic orthogneiss.|06-AUG-15
75920|Minigwal Suite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2769 +/- 8 Ma (isotopic) - 2765 Ma (inferred).||Includes Hope Campbell Orthogneiss, Baseline Orthogneiss, Surprise Orthogneiss|||
75920|Minigwal Suite|70802|5|Briefly described|500k_interpgeop14_lut.csv|||Geological province: Yilgarn Craton, West Australian Craton.|||Includes Baseline Orthogneiss, Hope Campbell Orthogneiss, Surprise Orthogneiss.|||
75920|Minigwal Suite|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Burtville Terrane, Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Edmundian Orogeny (1026 - 954 Ma); Mangaroon Orogeny (1682 - 1619 Ma); Stanley Fold Belt deformation (2005 - 1620 Ma); Mangaroon Orogeny D2m/M2m (1677 - 1659 Ma); Mangaroon Orogeny D1m/M1m (1682 - 1677 Ma). See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 100k_geologyp14_lut.csv, 500k_interpgeop_lut.csv, 2_5m_interpgeop15_lut.csv.|1876+\-19 Ma; 1650 Ma (inferred)||Includes Baseline Orthogneiss, Hope Campbell Orthogneiss, Surprise Orthogneiss.||Granitic gneiss.|
75920|Minigwal Suite|72034|6|Mentioned|500k_interpgeop16_lut|Neoarchean|Neoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Baseline Orthogneiss, Surprise Orthogneiss, Hope Campbell Orthogneiss.|||
24380|Mininer Turbidite Member|38321|6|Mentioned|p198|||||||||
24380|Mininer Turbidite Member|38790|6|Mentioned|p162|||||||||
24380|Mininer Turbidite Member|40937|6|Mentioned|p28|||||||||
24380|Mininer Turbidite Member|42260|6|Mentioned|p7|||||||||
24380|Mininer Turbidite Member|42277|6|Mentioned|Fig.1 P56|||||||||
24380|Mininer Turbidite Member|43037|5|Briefly described|Fig.2,p24|||of Ashburton Formation||||||
24380|Mininer Turbidite Member|61526|5|Briefly described|p880, p881|||Of the Ashburton Formation. See also the Mininer Turbidite (abbreviated version). Geological Province: Ashburton Basin.||||||
24380|Mininer Turbidite Member|70958|3|Fully described|p6-7, p11 App. 1, Fig. 1|Paleoproterozoic|Paleoproterozoic|Up to ~6000 m thick. Named after Mininer Station. Turee Creek map sheet area, N of Capricorn Ranges and Ashburton River and S of foothills of Hamersley Ranges. Said to be defined but no type section established.||Of Ashburton Formation.||Overlies Capricorn Member, but boundary is generalised and interfingering. Overlies Duck Creek Dolomite, interfingering in places.|Turbidites with well defined cyclicity; shales with grits, rafts of dolomite and grit|
24380|Mininer Turbidite Member|72712|6|Mentioned|p34.|Statherian|Orosirian|Of Horwitz (1980).Thorne and Seymour (1991) considered this name invalid despite their recognition of a three-fold subdivision of Ashburton Formation. Formerly considered to be a subdivision of the Ashburton Formation.||Ashburton Formation||Formerly considered to be a subdivision of the Ashburton Formation.|Includes turbidites.|
79473|Miningarra Group|69003|4|Described|p4, p13 Fig.17, p14-15|||Earaheedy Basin, Capricorn Orogen. Fine-grained, low-energy, shallow-marine deposits. Detrital zircon maximum depositional age (Mulgarra Sandstone).|c.1808 Ma.||Chiall, Wongawol Formations; Kulele Limestone; Mulgarra Sandstone.|Overlies Tooloo Group.|Turbidites, sandstone, limestone; contains stromatolites.|
79473|Miningarra Group|69596|5|Briefly described|p4, p10-11|Paleoproterozoic|Paleoproterozoic|Capricorn Orogen. A low-energy, shallow-marine succession. Appears as Minningarra Group on p4, p11 and p37.|||Chiall, Wongawol Formations; Kulele Limestone; Mulgarra Sandstone.|Disconformably overlies Tooloo Group.|Turbiditic sandstones and lesser carbonates.|
79473|Miningarra Group|70826|6|Mentioned|p6 tbl 2, p9|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin. May be a time equivalent of the Wyloo Group and the Leake Spring Metamorphics.||||Overlies the Tooloo Group.||
79473|Miningarra Group|71484|5|Briefly described|p122-124-125,130-131,137-138|||Geological province: Of Earaheedy Basin. Nomenclature by Martin et al., 2016; Sheppard et al., 2016; replacing (the now obsolete) Earaheedy Group, and Miningarra Subgroup (also now obsolete). Described a a major transgressive-regressive depositional package. Predominantly siliciclastic, with intermittent stromatolitic carbonate deposition.|||Incldues Mulgarra Sandstone, Kulele Limestone, Wongawol Fomation and Chiall Formation.|Underlain unconformably by Tooloo Group/Frere Formation.||30-AUG-19
79473|Miningarra Group|71798|6|Mentioned|p110|||Earaheedy Basin.||||||
79473|Miningarra Group|72034|6|Mentioned|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Mulgarra Sandstone, Kulele Limestone, Wongawol Formation, Chiall Formation.|||
78985|Minjar Member|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton.|c.2947 Ma.|Gossan Hill Formation.|||Felsic volcaniclastic rocks and fine-grained siliciclastic sedimentary rocks; minor amygdaloidal basalt; metamorphosed.|
78985|Minjar Member|70796|5|Briefly described|100k_geologyp_lut.csv|Mesoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. See also 100K_interpgeop_lut.csv, 500k_interpgeop_lut.csv, Badja100_2240_stratig.pdf. Numerous additional lithologies are discussed.|2946 +/ 4 Ma (isotopic)|Gossan Hill Formation|||Felsic volcaniclastic rocks and finegrained siliciclastic sedimentary rocks; minor amygdaloidal basalt; metamorphosed|
78985|Minjar Member|71269|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). Sample GSWA 211102 (felsic volcaniclastic rock) yielded a weighted mean 207Pb/206Pb date of 2947+\-4 Ma, interpreted as the magmatic crystallization age of the protolith of the felsic volcaniclastic rock. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv.|2947+\-4 Ma (isotopic)|Unit of Gossan Hill Formation.|||Felsic volcaniclastic rocks and fine-grained siliciclastic sedimentary rocks; basalt, commonly with 1--2 mm plagioclase phenocrysts; locally abundant amygdaloidal basalt and minor basaltic andesite; metamorphosed|
78985|Minjar Member|71272|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c.2947 Ma.|Gossan Hill Formation.|||Felsic volcaniclastic rocks and fine-grained siliciclastic sedimentary rocks; minor amygdaloidal basalt; metamorphosed. (Separately mapped) basalt, locally abundant amygdaloidal basalt and minor basaltic andesite, metamorphosed.|
26276|Minjoo Salt|14228|6|Mentioned|p6 fig3|Late Ordovician|Late Ordovician|South Canning Basin.||Carribuddy Group||Overlies Bongabinni Formation. Is overlain by Nibil Formation.||
26276|Minjoo Salt|22753|5|Briefly described|Fig.3 p585|Ordovician|Ordovician|||||||
26276|Minjoo Salt|24449|6|Mentioned|p745|||Geological Province: Canning Basin.||||||
26276|Minjoo Salt|40837|2|Defined|p257 Fig. 4, p274|Downtonian|Downtonian|Of the Carribuddy Group - replacing Unit D of Carribuddy Formation. Max. thickness: 170m in Kidson No.1 drill core. See also Fig. 5 page insert (p258).||||||27-JAN-10
26276|Minjoo Salt|41215|6|Mentioned|Fig.4|||||||||
26276|Minjoo Salt|42030|6|Mentioned|p746|||||||||
26276|Minjoo Salt|43563|6|Mentioned|Fig.2,p5|||||||||
26276|Minjoo Salt|43599|6|Mentioned|p250, Fig.3||Caradocian|||||||
26276|Minjoo Salt|43656|6|Mentioned|Fig.2,p8|Caradocian|Caradocian|||||||
26276|Minjoo Salt|43666|6|Mentioned|p49,Table 2||Ordovician|||||||
26276|Minjoo Salt|43746|6|Mentioned|Fig.2,p11|Caradocian|Caradocian|||||||
26276|Minjoo Salt|43818|6|Mentioned|Fig.2.p39||Silurian|||||||
26276|Minjoo Salt|44143|4|Described|p.440 Table 4-19; p.442, Figure 4-96|Devonian|Silurian|Unit in Carribuddy Group. Up to 166m thick; halite with red-brown claystone & dolomite; sabkha and supratidal marine. Conformably overlies Bongabinni Formation; is overlain conformably by Nibil Formation. Type section between 3905 and  4071m in Kidson 1 (URAL: 22 deg 37' 27" S, 125 deg 00' 17" E). Contains sparse spores and pollen.||||||
26276|Minjoo Salt|61021|5|Briefly described|p36 Fig. 2|Caradocian|Caradocian|Thick evaporitic section. Geological Province: Canning Basin.||||||17-DEC-07
26276|Minjoo Salt|61551|5|Briefly described|p351 Fig.2, p359.|Late Ordovician|Late Ordovician|||Unit in Carribuddy Group.|||Evaporites.|
26276|Minjoo Salt|64334|5|Briefly described|p39|Ordovician|Ordovician|Canning Basin; subsurface only. Caradoc.||Carribuddy Group.||Overlies Bongabinni Formation. Is overlain by Nibil Formation.|Halite.|
26276|Minjoo Salt|64643|5|Briefly described|p3 Fig. 2|Late Ordovician|Late Ordovician|Of Carribuddy Group?||||||11-FEB-20
26276|Minjoo Salt|64982|5|Briefly described|p698.|Early Ordovician|Early Ordovician|Thickness to 160 m. Laterally equivalent to Mount Troy Formation.||Unit in Carribuddy Group.||Overlies Bongabinni Formation. Is overlain by Nibil Formation.|Halite with red-brown claystones.|
26276|Minjoo Salt|65301|5|Briefly described|p3, p5 Fig. 4|Late Ordovician|Late Ordovician|Geological province: Canning Basin, including Kidson Sub-basin and Broome Platform. Form a super-seal over underlying units||||||09-APR-13
26276|Minjoo Salt|65449|3|Fully described|p1, p6-8, p13-14, p18-23, p47-50, p56-57|Late Ordovician|Late Ordovician|See also Plates 1-4. Lehmann (1984), after Minjoo Native Well. Type section is the interval 4071-3905m in Kidson 1. From 19 to 313m thick. Age range from surrounding units.||Carribuddy Group.||Conformably and gradationally overlies Bongabinni Formation. Is overlain conformably and gradationally by Nibil Formation. Equivalent to Mount Troy Formation.|Red-brown calcareous and dolomitic mudstone, grading to argillaceous dolomite, with interbeds of reddish-brown to brown and colourless coarsely-crystalline halite; scattered crystals of halite; minor anhydrite.|
26276|Minjoo Salt|68007|3|Fully described|p1-2,p4-5,p7,p11-12, p14-15, Plates 1, 2|Late Ordovician|Late Ordovician|Canning Basin. 313m thick in Patience 2 well. Type section is in WAPET's Kidson 1 stratigraphic well. Forms a regional seal over the prospective Ordovician section. Gas shows downwards from the base of this unit. Composite well log.||Of Carribuddy Group.||Overlies Bongabinni Formation. Is overlain by Nibil Formation.|Coarsely crystalline, orange-brown to red-brown, clear to translucent halite interbedded with reddish-brown partly dolomitic claystone.|24-FEB-20
26276|Minjoo Salt|68902|5|Briefly described|p9 fig 5, p26|Ordovician|Ordovician |||Carribuddy Group||Overlies Bongabinni Formation, overlain by Nibil Formation.||
26276|Minjoo Salt|69029|6|Mentioned|p319|Late Ordovician|Late Ordovician|Of Canning Basin.||||Overlain by Nibil Formation. Underlain by Bongabinni Formation.||
26276|Minjoo Salt|69182|6|Mentioned|Ch4 p9-p12, Ch4 p38, Ch4 p40-p41|Upper Ordovician|Upper Ordovician|Canning Basin. This unit may act as a potential carbon dioxide seal. See also Ch4 p45, Ch4 p47, Ch4 p50-p58, Ch4 p74, Ch4 p79-p82, Ch4 p92, Ch4 p94. ||Carribuddy Group||Overlies the Bongabinni Formation. Overlain by the Nibil Formation.||
26276|Minjoo Salt|69312|6|Mentioned|p3, p24 fig 28|Late Ordovician|Middle Ordovician|Canning Basin. See also p25 fig 30, p27 fig 34, p28 fig 36. ||Carribuddy Group||Overlies the Bongabinni Formation. Overlain by the Nibil Formation.|Salt.|11-FEB-20
26276|Minjoo Salt|69883|5|Briefly described|p4-p5|Caradoc|Caradoc|Canning Basin. Supersequences provided. Marginal marine barred-basin setting.||Carribuddy Group||Overlies the Bongabinni Formation. Overlain by the Nibil Formation. Laterally equivalent to the Mount Troy Formation.|Halite deposits.|
26276|Minjoo Salt|70774|5|Briefly described|p4|Late Ordovician|Late Ordovician|Willara and Kidson Sub-basins, Canning Basin.||Carribuddy Group||Overlies the Bongabinni Formation. Overlain by the Nibil Formation.||06-FEB-20
26276|Minjoo Salt|71146|5|Briefly described|p6|Late Ordovician|Late Ordovician|Canning Basin.||Carribuddy Group|||Halite, evaporite.|
26276|Minjoo Salt|71171|6|Mentioned|p2|||Canning Basin.||||||
26276|Minjoo Salt|71870|6|Mentioned|p3|Katian|Sandbian|Canning Basin.||Carribuddy Group||Overlies the Bongabinni Formation. Overlain by the Nibil Formation.||
26276|Minjoo Salt|71894|5|Briefly described|p4|Late Ordovician|Late Ordovician|Canning Basin.||Carribuddy Group||Overlies the Bongabinni Formation. Overlain by the Nibil Formation.|Salt (evaporite).|11-FEB-20
26276|Minjoo Salt|72497|5|Briefly described|p3 Fig.2.|Katian|Sandbian|Shown as occuring in the Anketell, Tabletop, Ryan Shelves, Willara and Kidson Sub-basins, the Jurgurra and Barbwire Terraces and Broome Platform. Age shown as Caradocian= Gisbornian - Eastonian (Aust), Sandbian - Katian (ICS)||Carribuddy Group||Conformably overlies Bongabinni Formation and underlies Nibil Formation and is laterally equivalent to Mount Troy Formation.||
26276|Minjoo Salt|72499|5|Briefly described|p7 Fig.6.|Late Ordovician|Late Ordovician|Located in the Willara Sub-basin and the Broome Platform.||Carribuddy Group||Overlies Bongabinni Formation and underlies Nibil Formation.|Includes evaporites.|
26276|Minjoo Salt|73117|5|Briefly described|p3|Upper Ordovician|Upper Ordovician|Canning Basin.||Carribuddy Group||Underlain by Bongabinni Formation.|Dominantly evaporite, salt.|
26276|Minjoo Salt|73344|6|Mentioned|p6|Sandbian|Sandbian|Canning Basin, subsurface. Part of supersequence B1.||Carribuddy Group||Underlain by Bongabinni Formation. Overlain by Nibil Formation. Equivalent[?] to Mount Troy Formation.||
26276|Minjoo Salt|73346|6|Mentioned|p27|||||||||
35239|Minnamonica Monzogranite|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Of Carlindi Granitoid Complex. Geological Province: Pilbara Craton.||||||15-APR-13
35239|Minnamonica Monzogranite|24110|5|Briefly described|Plate 1|Archean|Archean|Belongs to Carlindi Granitoid Complex. Geological Province: Pilbara Craton||||||15-APR-13
35239|Minnamonica Monzogranite|24166|4|Described|p18|Archean|Archean|Of the Carlindi Granitoid Complex. Intruded by the Poocatche Monzogranite.||||||15-APR-13
35239|Minnamonica Monzogranite|24193|5|Briefly described|p876 Fig.3|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
35239|Minnamonica Monzogranite|24327|5|Briefly described|Map Legend|Archean|Archean|Of the Carlindi Granitoid Complex. Porphyritic biotite (-muscovite) monzogranite. Age: c. 2940 Ma. Geological Province: Pilbara Craton.||||||15-APR-13
35239|Minnamonica Monzogranite|24349|5|Briefly described|Map legend|Archean|Archean|Of the Carlindi Granitoid Complex. Age: c. 2940 Ma. Geological Province: Pilbara Craton.||||||15-APR-13
35239|Minnamonica Monzogranite|50379|5|Briefly described|Map Legend|Archean|Archean|Of Carlindi Granitoid Complex. Geological Province: Pilbara Craton.||||||07-NOV-08
35239|Minnamonica Monzogranite|63420|5|Briefly described|Map legend|Archean|Archean|Of Split Rock Supersuite. Geological Province: Pilbara Craton. Quartz and K-feldspar porphyritic muscovite (-biotite) monzogranite; fine- to coarse-grained; massive to weakly foliated.||||||07-NOV-08
35239|Minnamonica Monzogranite|63441|5|Briefly described|p12 tb. 2|Archean|Archean|Of Split Rock Supersuite. Geological province: Pilbara Craton.||||||07-FEB-11
35239|Minnamonica Monzogranite|66108|5|Briefly described|Map legend|Neoarchean|Neoarchean|Unit in Split Rock Supersuite. Quartz and K-feldspar porphyritic muscovite(-biotite) monzogranite; fine- to coarse-grained; massive to weakly foliated.||||||
35239|Minnamonica Monzogranite|68281|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.||Of the Split Rock Supersuite.|||Quartz and K-feldspar porphyritic muscovite(-biotite) monzogranite; fine to coarse grained; massive to weakly foliated.|02-DEC-14
35239|Minnamonica Monzogranite|68283|5|Briefly described|Map Legend|Mesoarchean||Pilbara Craton.||Of the Split Rock Supersuite.|||Quartz and K-feldspar porphyritic muscovite(-biotite) monzogranite; fine to coarse grained; massive to weakly foliated.|
35239|Minnamonica Monzogranite|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton. Age constrained by the parent Split Rock Supersuite.||Of the Split Rock Supersuite.|||Quartz and K-feldspar porphyritic muscovite(-biotite) monzogranite; fine to coarse-grained; massive to weakly foliated.|30-APR-14
35239|Minnamonica Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Quartz and K-feldspar porphyritic muscovite(--biotite) monzogranite; fine to coarse grained; massive to weakly foliated|
35239|Minnamonica Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; Split Rock Supersuite Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.|2851-2831 Ma (inferred)|Unit of Split Rock Supersuite.|||Quartz and K-feldspar porphyritic muscovite(--biotite) monzogranite; fine to coarse grained; massive to weakly foliated|
35239|Minnamonica Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
35239|Minnamonica Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Quartz and K-feldspar porphyritic muscovite(--biotite) monzogranite; fine to coarse grained; massive to weakly foliated.|
31965|Minnie Creek Granodiorite|24197|6|Mentioned|p71 Tb. 7.1|||Of the Minnie Creek Supersuite.||||||07-FEB-11
31965|Minnie Creek Granodiorite|50425|5|Briefly described|p1.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Province. Of the Minnie Creek Supersuite.||||||07-NOV-08
31965|Minnie Creek Granodiorite|63866|4|Described|p154|Statherian|Statherian|Numeric age is a SHRIMP U-Pb zircon age.|1795 +/- 8 Ma (Evans et al., 2003)|||||
74108|Minnie Creek Suite|24197|5|Briefly described|p26|Paleoproterozoic|Paleoproterozoic|Example of the Cullen Association. Age: ~1800Ma. Geological Province: Gascoyne Province. See also Minnie Creek Supersuite - names used interchangeably in this study.||||||07-FEB-11
31905|Minyari Granite|24197|5|Briefly described|p26, p102 Tb. 14.1|Neoproterozoic|Neoproterozoic|Of O'Callaghan's Supersuite. I-type (granodioritic) Minyari type granite. Age: ~625Ma. Geological province: Paterson Province.||||||27-SEP-12
31905|Minyari Granite|24594|5|Briefly described|p608 Fig. 4|Neoproterozoic|Mesoproterozoic|Age: ~650Ma (U-Pb zircon, Nelson 1995).  Geological Province: Paterson Orogen.||||||
31905|Minyari Granite|50436|5|Briefly described|p1.3, 4.1, Table 1.1|Neoproterozoic|Neoproterozoic|Geological Province: Paterson Orogen. Of the Minyari Group (O'Callaghans Supersuite).  Age: 633 +/- 13Ma (U-Pb).|||||monzogranite to syenogranite|27-SEP-12
31905|Minyari Granite|67202|5|Briefly described|p189, p191|||A unit in the Minyari group of granites (a subdivision of the O'Callaghans Supersuite by Goellnicht et al., 1991); assigned to the O'Callaghans Suite by Wyborn (1997) and Budd et al. (2001). Geochronology by Maidment, unpub. data in Czarnota et al. (2009).|c.630 Ma.|O'Callaghans Suite.||||
31905|Minyari Granite|68902|6|Mentioned|p12, p14, p17|||A string of concealed plutons extends NW from this unit, possibly associated with deep-seated transfer or rift-border faults. Appears also as Minyai Granite on p17.||||||
31905|Minyari Granite|69873|6|Mentioned|p91|||Considered by Budd et al., (2001) to have some similarities with Proterozoic granites on King Island (Tas), with implications for Au/Cu mineralisation.||||||
32214|Miralga Creek Member|23755|5|Briefly described|p34|Archean|Archean|Of Euro Basalt.||||||07-NOV-08
32214|Miralga Creek Member|24531|6|Mentioned|p18|||On the NORTH SHAW sheet.||||||
32214|Miralga Creek Member|24590|6|Mentioned|p130 Fig.4.1|||||||||07-FEB-11
32214|Miralga Creek Member|61266|4|Described|p57|Archean|Archean|Of the Euro Basalt. Pillowed tholeiitic basalts and interbedded cherts. Overlies the Cloisters Member and Strelley Pool Chert. Geological Province: Pilbara Craton.||||||07-NOV-08
27835|Miranda Member|41199|4|Described|p22|||See also Table 1. Of Darlot Formation.||||||
27835|Miranda Member|43065|6|Mentioned|p93|||of Darlot Formation||||||
75368|Mirrabooka Member|12759|2|Defined|p39; p28 Tb. 7; p32 Fig 15; P36 Fig 17|Cenomanian|Albian|New name. Named from: Mirrabooka suburb, N of Perth. No connection with Mirrabooka Formation (NSW). Type Section: Bore AM30Z, between 34-199 m depth (max 160 m) at AMG Zone 50 (397560m E, 6478832m N).||Of Osborne Formation.||Conformably overlain by Molecap Greensand. Conformably underlain by Kardinya Shale Member.|Sandstone, dark greenish brown, very poorly sorted, silty and richly glauconitic; with thin interbeds of siltstone and shale, dark green to black, glauconitic.|12-MAY-14
75368|Mirrabooka Member|14227|5|Briefly described|Enclos. 2|Late Cretaceous|Late Cretaceous|Of Coolyena Group. Probably of Osborne Formation. Presented as Mirrabooka Mem.||||||07-FEB-11
75368|Mirrabooka Member|67115|6|Mentioned|p64, p65 Fig. 3 |Cretaceous|Cretaceous|Lithology and trace elements detailed.||Osborne Formation||Overlies the Pinjar Member (Leederville Formation).|Sandstones.|
75368|Mirrabooka Member|68254|6|Mentioned|p1036 Fig.2, p1039, p1040 Tb.3|Cretaceous|Cretaceous|||Of the Osborne Formation.||||
73625|Mirturtu Monzogranite|64408|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Subdivided into 6 unnamed units. Of Pitjantjatjara Supersuite. Geol. Province - Musgrave Complex.||||||03-MAY-13
73625|Mirturtu Monzogranite|66284|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province.||||Includes interleaves from Birksgate Metamorphics.|Pyroxene-biotite-hornblende metamonzogranites, locally charnokitic protolith, locally rapakivi texture; hornblende-garnet granodioritic augen gneiss, strongly foliated to blastomylonitic; lesser metagranodiorite to quartz monzodiorite.|
73625|Mirturtu Monzogranite|67375|5|Briefly described|p151, pp180-181.|Mesoproterozoic|Mesoproterozoic|Often used interchangeably with the term Mirturtu Suite. The only geochemically-coherent suite within the Pitjantjatjara Supersuite that is distinguishable on the current 1:100 000 series maps (BATES; Howard et al., 2006).||Unit in Pitjantjatjara Supersuite.|||Monzogranite, ranging from granodiorite to syenogranite; charnockite; unfoliated to strongly foliated and mylonitized; local relict rounded rapakivi-textured feldspar phenocrysts to 5 cm diameter.|
73625|Mirturtu Monzogranite|67553|6|Mentioned|p70,75|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province, North Australian Craton.||Unit of Pitjantjatjara Supersuite.|||Pyroxene-biotite-hornblende metamonzogranite and hornblende-garnet granodioritic augen gneiss.|
73625|Mirturtu Monzogranite|70793|5|Briefly described|180256.1.pdf|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Sample GSWA 180256 (metagranodiorite) yielded an interpreted (uncorrected U/Pb and Pb/Pb) best estimate age of igneous crystallisation and maximum age of granulite metamorphism at 1176+\-6 Ma. ||Unit of Mirturtu Suite.||||
73625|Mirturtu Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, granodiorite, quartz monsodiorite, charnockite, granodioritic augen gneiss|
73625|Mirturtu Monzogranite|71268|4|Described|1m_geologyp12_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Metamorphosed to granulite facies. Sample GSWA 174538 (porphyritic metamonzogranite) yielded 238U/206Pb and 207Pb/206Pb concordia ages of 1178+\-8 Ma, interpreted to be crystallisation age of igneous protolith. Sample GSWA 180256 (metamorphosed granodiorite) yielded a regression line intersecting concordia curve at 1176+\-6 Ma, interpreted as the best estimate of the age of igneous crystallization of the precursor granodiorite, and a maximum age for granulite facies metamorphism. Sample GSWA 180299 (porphyritic granite) yielded a weighted mean 207Pb/206Pb age of 1175+\-15 Ma, interpreted as igneous crystallisation age of the precursor granite. Sample GSWA 180300 (porphyritic metamonzogranite) yielded a weighted mean 207Pb/206Pb age of 1181+\-6 Ma, interpreted as igneous crystallisation age of the precursor monzogranite.|1178+\-8 Ma; 1175+\-15 Ma; 1181+\-6 Ma|Unit of Mirturtu Suite.|||Metamonzogranite, metagranodiorite, metaquartz-monzodiorite, hornblende-garnet granodioritic augen gneiss; charnockite; rapakivi granite; garnet coronas around mafic minerals; locally mylonitic.|
74764|Mirturtu Suite|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Mapped as two separate but un-named units.||Unit in Pitjantjatjara Supersuite.|||Pyroxene-biotite-hornblende metamonzogranite, locally mylonitised +/- charnockite protolith and rapakivi texture; lesser metagranodiorite to quartz monzodiorite; typically has garnet coronas around mafic minerals; seriate to K-feldspar porphyritic.|
74764|Mirturtu Suite|67375|4|Described|pp180-186.|Mesoproterozoic|Mesoproterozoic|Often used interchangeably with the term Mirturtu Monzogranite. Is said to be the only geochemically coherent Suite subdivision of the Pitjantjatjara Supersuite on the current 1:100 000 geological maps, and yet "there appears to be no significant lithological difference between the rocks of the Mirturtu Monzogranite and any other rocks of the late Pitjantjatjara Supersuite".|1183 +/- 9 - 1176 +/- 6 Ma (Bodorkos et al. 2008).|||Locally includes Wirku Metamorphics.|Monzogranite, granodiorite, syenogranite, charnockite, hornblende-garnet granodioritic augen gneiss; pyroxene-biotite-hornblende monzogranite, locally mylonitized|
74764|Mirturtu Suite|69153|5|Briefly described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Paterson Orogen, Musgrave Province. Note misspelt member, Miturtu Monzogranite, has Geochron analyses of zircons.||Pitjantjatjara Supersuite|||Hornblende-garnet granodioritic augen gneiss; (mylonitic) pyroxene-biotite-hornblende metamonzogranite; minor metamorphosed granodiorite to quartz monzodiorite|
74764|Mirturtu Suite|69436|5|Briefly described|p21:8|||Howard et al. (2011). May be related to the Umutju Suite in adjacent regions in the NT.|c.1180 Ma.|||||12-JUL-16
74764|Mirturtu Suite|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|Musgrave Province/(Complex?),|1176 Ma - 1183 Ma (Inferred)|Pitjantjatjara Supersuite|||Hornblende-garnet granodioritic augen gneiss, composite gneiss with interleaves and inclusions derived from Wirku Metamorphics units; pyroxene-biotite-hornblende metamonzogranite, metamorphosed granodiorite to quartz monzodiorite.|
74764|Mirturtu Suite|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. [Also known as Mirtutu Monzogranite Suite]. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma); Musgrave Orogeny (1220-1150 Ma). Sample GSWA 174538 (metamonzogranite) yielded an interpreted (Pb/Pb, U/Pb concordia line intersecting regression curve) igneous crystallisation age of 1178+\-8 Ma. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv.|1183+\-9 Ma; 1176+\-6 Ma|Unit of Pitjantjatjara Supersuite.|Includes Mirturtu Monzogranite.||Hornblende-garnet granodioritic augen gneiss; mylonitic pyroxene-biotite-hornblende metamonzogranite; k-feldspar porphyritic (rapakivi granite) and locally charnockitic protolith, minor metamorphosed granodiorite to quartz monzodiorite.|
74764|Mirturtu Suite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 1m_geologyp12_lut.csv.|1183+\-9 Ma; 1176+\-6 Ma|Unit of Pitjantjatjara Suite.|Includes Mirturtu Monzogranite.||Hbl-gt granodioritic augen gneiss; px-bt-hbl metamonzogranite and minor metamorphosed granodiorite to quartz monzodiorite; K-feldspar porphyritic (rapakivi granite) and locally charnockitic protolith.|
23801|Missouri Basalt|22534|5|Briefly described|p4, Fig.4 p7|||of Pole Group, See also Table 2. p8||||||
23801|Missouri Basalt|22596|6|Mentioned|Fig.9 p419|||||||||
23801|Missouri Basalt|22640|5|Briefly described|p298|||||||||
23801|Missouri Basalt|42221|6|Mentioned|Table 1 P6|||||||||
23801|Missouri Basalt|42382|5|Briefly described|Fig.4 P11|||||||||
23801|Missouri Basalt|42436|6|Mentioned|Fig.2 P.75|||||||||
23801|Missouri Basalt|42696|6|Mentioned|Plate 1B|Archean||||||||07-NOV-08
23801|Missouri Basalt|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
23801|Missouri Basalt|42870|5|Briefly described|Table 1, P67|||||||||
23801|Missouri Basalt|42989|5|Briefly described|Fig.3|||||||||
23801|Missouri Basalt|43074|6|Mentioned|Fig.4|||||||||
23801|Missouri Basalt|43101|5|Briefly described|p12|||0f Pole Group||||||
23801|Missouri Basalt|43162|6|Mentioned|5|||||||||
23801|Missouri Basalt|43574|5|Briefly described|Fig.1,p298|||||||||
23801|Missouri Basalt|60076|5|Briefly described|p12 Tb. 2|||Massive to pillowed porphyritic basalt.  Max. thickness: <1500m.  Geological Province: Ora Banda domain.||||||
23801|Missouri Basalt|60514|6|Mentioned|p65 Table 1.|Archean|Archean|Of the Pole Group. Overlain by Linger and Die Group, underlain by Wongi Basalt. Geological Province: Ora Banda Domain.||||||07-FEB-11
23801|Missouri Basalt|60627|5|Briefly described|p65 Tb.1|||Of Pole Group||||||
23801|Missouri Basalt|63981|6|Mentioned|p93 Fig.3, |Archean|Archean|Ora Banda Domain. Kambalda Sequence. |||||Tholeiitic and high MgO basalt.|
23801|Missouri Basalt|64771|5|Briefly described|p9|||Swager et al. (1995). Ghost Rocks area.|||||Basaltic schist, passing into metagabbro and cumulate-textured metapyroxenite.|
23801|Missouri Basalt|65204|5|Briefly described|pg6 Tbl.1, p10-11,|Archean|Archean|Unit in Pole Group. Ora Banda Domain. Tholeiitic basalt; quartz-filled amygdales are characteristic of the upper part; may be feldspar-phyric with fine- to medium-grained plagioclase phenocrysts.||||||11-JUN-15
23801|Missouri Basalt|65834|6|Mentioned|p7, 13|||Ora Banda Domain, Kalgoorlie Terrane.||Pole Group.||||
23801|Missouri Basalt|69631|5|Briefly described|p49|||Swager et al. (1995).|||||Basaltic schist, passing into metagabbro and cumulate-textured metapyroxenite.|
23801|Missouri Basalt|70326|5|Briefly described|p360-362,365|Neoarchean|Neoarchean|Geological province: Ora Banda region, Ora Banda Domain, Kalgoorlie Terrane, Yilgarn Craton.||||Overlain by Walter Williams Formation. Underlain by Wongi Basalt. Correlable to Never Can Tell Basalt.||
23801|Missouri Basalt|70773|5|Briefly described|p48|||Name derived from Swager et al., 1995.|||||Basaltic schist.|
23801|Missouri Basalt|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).  See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2726-2680 Ma (inferred)|Unit of Vetters Subgroup.|||Tholeiitic basalt and intercalated subordinate high-magnesium basalt, plagioclase-phyric basalt; massive to pillowed; metamorphosed; fine- to medium-grained amphibolite, typically foliated.|
23801|Missouri Basalt|73391|5|Briefly described|p17, 53, 279, Appendices.|||Ora Banda Domain, Eastern Goldfields Province. Shown as having a combined thickness over 3000m with Wongi Basalt.||Pole Group; Lower Basalt.||Overlies Siberia, Owen Monzogranites. Is overlain by Walter Williams dunite.|Poorly exposed basalt and amphibolite; intercalated with felsic sedimentary rocks.|
23801|Missouri Basalt|73596|6|Mentioned|p1160|||Appears as Lunnon/Missouri Basalt.||||||
22353|Mistico Formation|61217|5|Briefly described|p20 Fig. 1|||In the Mount Magnet greenstone belt.||||||07-FEB-11
22353|Mistico Formation|61853|5|Briefly described|p328|||Geological Province: Yigarn Craton.||||||03-JUL-06
22353|Mistico Formation|69744|6|Mentioned|p256, 259, p261 Fig.6|||Mount Magnet Greenstone Belt.|c.2720 Ma.||||Felsic volcanics, cherts and clastic sediments.|
36988|Mitchell Porphyry|23470|5|Briefly described|p125|Archean|Archean|Age: 2678+/-5 Ma. Geological Province: Yilgarn Craton.||||||07-NOV-08
26035|Molecap Greensand|12758|5|Briefly described|p22, p3 Fig. 3|Cretaceous|Cretaceous|Of the Coolyena Group.||||||
26035|Molecap Greensand|12759|3|Fully described|p39; p28 Tb. 7; p32 Fig 15; P36 Fig 17|Santonian|Turonian|Defined Fairbridge (1953); Type section in the greensand quarry  on Molecap Hill, 2km S of Gingin (AMG Z50, 347832 m E, 6528643 m N). Max thickness is 80m.||Of Coolyena Group.||Conformably (transitionally) overlies Mirrabooka Member (Osborne Formation); is overlain conformably by the Gingin Chalk or unconformably by Poison Hill Greensand.|Fine- to medium-grained, yellow-brown to greenish-grey, glauconitic, silty, locally clayey sandstone; phosphatic nodules common in upper part. Mostly unconsolidated.|12-MAY-14
26035|Molecap Greensand|14227|5|Briefly described|Enclos. 2|Late Cretaceous|Late Cretaceous|Of Coolyena Group.||||||07-FEB-11
26035|Molecap Greensand|23279|6|Mentioned|p31|||||||||
26035|Molecap Greensand|23816|4|Described|p248|Late Cretaceous|Late Cretaceous|Geological Province: Perth Basin. Of the Coolyena Group. Conformably underlain by Osborne Formation. Conformably overlain by Gingin Chalk. Max. thickness: 12 m.||||||05-MAR-08
26035|Molecap Greensand|24085|6|Mentioned|p40|||||||||
26035|Molecap Greensand|24094|5|Briefly described|p268|Cretaceous|Cretaceous|Geological Province: Perth Basin.||||||16-MAR-05
26035|Molecap Greensand|24160|6|Mentioned|p95 Tb.57.|Late Cretaceous|Late Cretaceous|||||Overlies Osborne Formation. Is overlain by Gingin Chalk.||
26035|Molecap Greensand|29382|6|Mentioned|Table 10|||||||||
26035|Molecap Greensand|29693|6|Mentioned|p66|||||||||
26035|Molecap Greensand|30188|2|Defined|p75|Late Cretaceous|Late Cretaceous|Refers Fairbridge(1953).||||||
26035|Molecap Greensand|30244|6|Mentioned|p142|||Cretaceous age||||||
26035|Molecap Greensand|31153|6|Mentioned|Fig. 57|||Stratigraphic table. Refers Cockbain & Playford (1973)||||||
26035|Molecap Greensand|31238|6|Mentioned|Fig. 12A|||||||||
26035|Molecap Greensand|31396|6|Mentioned|p1183|||See also P1184||||||
26035|Molecap Greensand|31562|5|Briefly described|p11|||||||||
26035|Molecap Greensand|32391|6|Mentioned|p1|||||||||
26035|Molecap Greensand|32648|6|Mentioned|p32|||U. Cret.||||||
26035|Molecap Greensand|33044|4|Described|p44|||Diagrams 16 and 21.||||||05-MAR-08
26035|Molecap Greensand|33165|6|Mentioned|Chart|||Correlation chart only||||||
26035|Molecap Greensand|34112|6|Mentioned|p3|||Upper Cretaceous||||||
26035|Molecap Greensand|34413|6|Mentioned|p13|||Senonian||||||
26035|Molecap Greensand|34414|6|Mentioned|p53|||Senonian||||||
26035|Molecap Greensand|34721|6|Mentioned|p286|||||||||
26035|Molecap Greensand|35026|6|Mentioned|p331|||||||||
26035|Molecap Greensand|35057|5|Briefly described|p301|||||||||
26035|Molecap Greensand|35282|6|Mentioned|Fig.2|||See also P30.||||||
26035|Molecap Greensand|35638|6|Mentioned|Map legend|Late Cretaceous|Late Cretaceous|||||||
26035|Molecap Greensand|35968|5|Briefly described|p64|||See also Fig.8.||||||
26035|Molecap Greensand|35970|6|Mentioned|Table 12|||||||||
26035|Molecap Greensand|35973|5|Briefly described|p94|||||||||
26035|Molecap Greensand|36257|6|Mentioned|Table 2.1|||||||||
26035|Molecap Greensand|36265|5|Briefly described|Fig.3.26|Late Cretaceous|Late Cretaceous|Of the Coolyena Group. Geological province: Perth Basin.||||||04-MAR-08
26035|Molecap Greensand|36293|2|Defined|p180|Late Cretaceous|Late Cretaceous|||||||
26035|Molecap Greensand|36865|6|Mentioned|p605|||||||||
26035|Molecap Greensand|36890|3|Fully described|p250|||||||||
26035|Molecap Greensand|37104|6|Mentioned|Fig.3|||||||||
26035|Molecap Greensand|37577|6|Mentioned|p67|||||||||
26035|Molecap Greensand|38221|6|Mentioned|Fig.4|||Perth Basin||||||
26035|Molecap Greensand|38444|6|Mentioned|p300|||See also P301.||||||
26035|Molecap Greensand|39211|6|Mentioned|Fig.38|||See also correlative P66||||||
26035|Molecap Greensand|40348|6|Mentioned|Map legend|Late Cretaceous|Late Cretaceous|||||||
26035|Molecap Greensand|40349|5|Briefly described|p17|||||||||
26035|Molecap Greensand|41341|6|Mentioned|p51|||||||||
26035|Molecap Greensand|42001|6|Mentioned|Fig.2 P79|||||||||
26035|Molecap Greensand|42123|4|Described|p21|||||||||
26035|Molecap Greensand|42995|5|Briefly described|Table 1|||||||||
26035|Molecap Greensand|43252|6|Mentioned|p163|||||||||
26035|Molecap Greensand|43347|6|Mentioned|9|||||||||
26035|Molecap Greensand|43700|6|Mentioned|p25|||||||||
26035|Molecap Greensand|44144|4|Described|p503 Tb.4-21, p517|Santonian|Cenomanian|Type Section: Molecap Hill 31o22'S 115o24'E. 12m thick marine shelf deposits with ichthyosaur, plesiosaur, mosasaur remains.||Coolyena Group||Overlies Osborne Formation conformably. Overlies Dandaragan Sandstone or Leederville Formation disconformably. Overlain by Gingin Chalk conformably.|Green to brown, fine- to medium-grained greensand and glauconitic sandstone.|
26035|Molecap Greensand|46883|6|Mentioned|p211|||||||||
26035|Molecap Greensand|61811|4|Described|p3 Fig.2, pp54-57, p64.|Turonian|Albian|Northern Perth Basin. Type section is in Molecap Hill Quarry, 1.4 km S of Gingin; further details in Appendix 1. Clasts occur in breccia associated with the Yallalie impact structure. Up to 7 m thick. Upper 2 metres contain mosasaur, ichthyosaur and plesiosaur remains. Formerly quarried as a source of glauconite as a water-softening agent.||Unit in Coolyena Group.||Overlies Osborne Formation, and unconformably overlies Leederville Formation (of the Warnbro Group). Is overlain by Lancelin Formation and Gingin Chalk.|Massive unit of coarse- to granule-sized quartz, and medium-sized dark-green glauconite, sandstone; phosphate nodules near the top.|
26035|Molecap Greensand|64580|6|Mentioned|map legend|||Of Coolyena Group.||||||15-DEC-08
26035|Molecap Greensand|64635|5|Briefly described|p4 Fig.3, |Coniacian|Cenomanian|||Unit in Coolyena Group.||||
26035|Molecap Greensand|67115|6|Mentioned|p64 Fig. 2 |Cretaceous|Cretaceous|||||Overlies the Osborne Formation, underlies the Lancelin Formation.||
26035|Molecap Greensand|67340|6|Mentioned|p6|Late Cretaceous|Late Cretaceous|Northern Perth Basin.||Coolyena Group.||||
26035|Molecap Greensand|68254|6|Mentioned|p1036 Fig.2, p1046 Tb.4|Cretaceous|Cretaceous|||||||
26035|Molecap Greensand|69182|6|Mentioned|Ch2 p9, Ch2 p45, Ch2 p55, Ch2 p57|Upper Cretaceous|Upper Cretaceous|Perth Basin. ||Coolyena Group||Overlies the Osborne Formation. Overlain by the Gingin Chalk and the Lancelin Formation.||
26035|Molecap Greensand|69297|6|Mentioned|p175, p189|Santonian|Turonian|Vlaming Sub-basin, South Perth Basin. ||Coolyena Group||Overlies the Osborne Formation. Overlain by the Gingin Chalk.||
26035|Molecap Greensand|70097|5|Briefly described|p20 Fig.4|Turonian|Albian|Northern Perth Basin. Dandaragan Trough.||Coolyena Group||Overlies Osborne Formation. Is overlain by Gingin Chalk.|Sandstone.|12-SEP-17
26035|Molecap Greensand|70099|5|Briefly described|Fig.4; p6|Coniacian|Turonian|Southern Perth Basin. Shallow marine sediments. Equivalent in age to deep marine, carbonate-dominated sedimentation of Mentelle 9 Supersequence.||Coolyena Group.||Overlies Osborne Formation. Is overlain by Gingin Chalk.||
26035|Molecap Greensand|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, claystone, phosphorite, greensand|
26035|Molecap Greensand|71790|6|Mentioned|p103|||Palynology p. 103.||||||
41171|Mondana Monzogranite|50381|5|Briefly described|Map Legend|Archean|Archean|Of Corunna Downs Granitoid Complex. Geological Province: Pilbara Craton. Lithology: very fine- to medium-grained leucogranite; quartz rich, minor biotie; equigranular to sparsely feldspar porphyritic.||||||07-NOV-08
41171|Mondana Monzogranite|63417|5|Briefly described|Map legend|Archean|Archean|Of Split Rock Supersuite. Geological Province: Pilbara Craton. Massive leucocratic monzogranite; very fine- to medium-grained; quartz-rich, minor biotite; equigranular to sparsely feldspar-phyric; metamorphosed.||||||07-NOV-08
41171|Mondana Monzogranite|63441|5|Briefly described|p8 Tb. 2|Archean|Archean|Of Emu Pool Supersuite. Supersedes Mondana Adamellite. Age: 3317+/-2Ma (Barley & Pickard, 1999). Geological province: Pilbara Craton.||||||06-APR-16
41171|Mondana Monzogranite|64327|5|Briefly described|p63 Fig. 2, p64|Archean|Archean|Originally defined as "Mondana Adamellite".  Intruded both Triberton Granodiorite and Boobina Porphyry. Fine- to medium-grained and leucocratic, and includes abundant quartz-rich aplite dykes.||||||07-NOV-08
41171|Mondana Monzogranite|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Corunna Downs Granitoid Complex. Geological Province: Pilbara Craton. Very fine- to medium-grained leucogranite; quartz rich, minor biotite; equigranular to sparsely feldspar porphyritic; metamorphosed.||||||07-FEB-11
41171|Mondana Monzogranite|65008|4|Described|p7, p12|Paleoarchean|Paleoarchean|East Pilbara Granite-Greenstone Terrane. Outcrops as a series of narrow bodies along the northeastern margin of the Corunna Downs Granitoid Complex.|ca. 3300 Ma|Of the Corunna Downs Granitoid Complex||Intrudes the Boobina Porphyry.|Very fine- to medium-grained leucogranite; quartz rich, minor biotite; equigranular to sparsely feldspar porphyritic; metamorphosed.|
41171|Mondana Monzogranite|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||Of Corunna Downs Granitoid Complex.|||Leucogranite; very fine- to medium-grained, quartz rich, minor biotite; equigranular to feldspar porphyritic.|
41171|Mondana Monzogranite|65727|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Pilbara Craton. In Version 1 of this map sheet, this unit was part of the Corunna Downs Granitoid Complex.||Of Split Rock Supersuite. |||Massive leucocratic monzogranite; very fine- to medium-grained, quartz rich, minor biotite; equigranular to sparsely feldspar porphyritic; weakly metamorphosed.|
41171|Mondana Monzogranite|65827|4|Described|p6 Tb.2, p9 Fig.3, p12 Tb.3, p15-16, p29|Mesoarchean|Mesoarchean|Of Split Rock Supersuite. Formerly Mondana Adamellite (Hickman and Lipple 1978). At c.2830 Ma, intrudes Corunna Downs Granitic Complex, Carbana Monzogranite, Panorama Formation (also adjacent to). Very fine to medium-grained leucogranite with abundant qtz-rich aplite dykes. Compositionally similar to Moolyella Monzogranite.||||||
41171|Mondana Monzogranite|66108|5|Briefly described|Map legend|Neoarchean|Neoarchean|Unit in Split Rock Supersuite. Massive leucocratic monzogranite; very fine- to medium-grained; quartz-rich, minor biotite; equigranular to sparsely feldspar-porphyritic; weakly metamorphosed.||||||
41171|Mondana Monzogranite|69012|5|Briefly described|Map Legend|Neoarchean|Mesoarchean|A micromonzogranite dyke of this unit is mapped separately.||Of the Split Rock Supersuite.|||Comprises massive leucocratic monzogranite; very fine to medium grained; quartz-rich, minor biotite; equigranular to sparsely feldspar-porphyritic; weakly metamorphosed.|29-APR-14
41171|Mondana Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Massive leucocratic monzogranite; very fine to medium grained; quartz-rich, minor biotite; equigranular to sparsely feldspar-porphyritic; weakly metamorphosed; micromonzogranitic dyke.|
41171|Mondana Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; Split Rock Supersuite Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.|2851-2831 Ma (inferred)|Unit of Split Rock Supersuite.|||Massive leucocratic monzogranite; very fine to medium grained; quartz-rich, minor biotite; equigranular to sparsely feldspar-porphyritic; weakly metamorphosed; micromonzogranite dyke|
41171|Mondana Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
41171|Mondana Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Massive leucocratic monzogranite; very fine to medium grained; quartz-rich, minor biotite; equigranular to sparsely feldspar-porphyritic; weakly metamorphosed.|
31885|Monkey Yard Tonalite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of Dougalls suite.  Age c. 1850 Ma||||||07-NOV-08
31885|Monkey Yard Tonalite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tickalara Metamorphics (Lamboo Complex).  Age: 1865-1850Ma.||||||07-NOV-08
31885|Monkey Yard Tonalite|43854|5|Briefly described|Map Legend||Proterozoic|of Tickalara Metamorphics.||||||
31885|Monkey Yard Tonalite|43855|5|Briefly described|Map Legend||Proterozoic|||||||
31885|Monkey Yard Tonalite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31885|Monkey Yard Tonalite|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Dougalls Suite.||||||07-NOV-08
31885|Monkey Yard Tonalite|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Tickalara Metamorphics. Age: c.1850Ma. Foliated and metamorphosed hornblende-biotite (-epidote) tonalite; epidote amphibolite inclusions.||||||
31885|Monkey Yard Tonalite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Tickalara Metamorphics.|||Foliated and metamorphosed hornblende-biotite(-epidote) tonalite; inclusions of epidote amphibolite|
73590|Mons Cupri Dacite Member|63441|5|Briefly described|p5 Tb.1|Archean|Archean|Of Red Hill Volcanics (Whim Creek Group, De Grey Supergroup), which together with this dacite member were formerly called Mons Cupri Volcanics. Geological province: Gorge Creek Basin, Pilbara Craton.||||||07-FEB-11
73590|Mons Cupri Dacite Member|67201|5|Briefly described|p64-66|||High level dacite intrusion.||Red Hill Volcanics.|||Dark grey dacite, wholly coherent and contains: a spherulitic matrix indicative of high temperature devitrification of volcanic glass; plagioclase phenocrysts and abundant, cherty fragments.|24-NOV-16
73590|Mons Cupri Dacite Member|70775|5|Briefly described|p51-p52, p81|||The precise stratigraphic relationships between this 'member' and the Cistern Formation remain somewhat ambiguous. See references for the Mount Brown Rhyolite [which this unit ostensibly supersedes]. Petrography is discussed briefly. This unit has not been dated but may be c. 30 million years younger than the Red Hill Volcanics and thus not a part of the Whim Creek Group. Alternatively multiple intrusive dacite units of varying ages may have been erroneously mapped as Mons Cupri Dacite Member.||Red Hill Volcanics|||Cream-coloured to grey spherulitic and feldspar-porphyritic dacite.|
73590|Mons Cupri Dacite Member|72668|6|Mentioned|p14|||Of Pike et al, 2002. Modelled as a deep crustal melt.||Red Hill Volcanics.||Coeval with the Warambie Basalt.||
73396|Monument Granite|65180|5|Briefly described|map legend|Archean|Archean|Hornblende or biotite bearing monzogranite to granodiorite of the Yilgarn Craton.||||||24-NOV-09
73396|Monument Granite|69152|4|Described|minerie_lut. files||Archean|Laverton Domain, Kurnalpi Terrane, Yilgarn Craton|||Includes 5 unnamed subunits.||Granitic rock, undivided; includes deeply weathered rock; equigranular hornblende granodiorite; monzogranite; variously biotite bearing, equigranular, megacrystic, porphyritic.|06-AUG-15
73396|Monument Granite|70153|5|Briefly described|Minerie_100k_geologyp_lut.csv|Archean|Archean|See also minerie_100k_interpgeop_lut. csv. Laverton Domain, Kurnalpi Terrane.|||||Granitic rocks. Equigranular hornblende granodiorite; monzogranites: equigranular, porphyritic and megacrystic varieties, also biotite-bearing with local hornblende, common K-feldspar megacrysts.|
73396|Monument Granite|71270|5|Briefly described|minerie_100k_geologyp_lut.csv|||Geological province: Laverton Domain, Kurnalpi Terrane, Yilgarn Craton, West Australian Craton.|||||Hornblende granodiorite, monzogranite: locally porphyritic, megacrystic, biotite-bearing; undivided granitic rock.|
80583|Moodagara Dolerite|72712|5|Briefly described|p9, p36, p38, p40, p38 Fig.27.|Orosirian|Rhyacian|New. Age inferred from units intruded, and younger (P-d5, Panhandle Dolerite dykes c. 2008 Ma). Equivalent to the P-d4 west-northwesterly trending dolerite dykes of Tyler (1990, 1991).|2008 Ma.|||Intrudes all strata up to and including Nummana Member, Cheela Springs Basalt, top Shingle Creek Group. Identified in the Turee Creek Group.|Dolerite dykes.|
79174|Moodini Supersuite|70748|6|Mentioned|p50|Stenian|Stenian|Madura Province. Similar in age to the Eyre 1 granite.|c. 1180-1125 Ma (Wingate et al, 2015b)|||||
79174|Moodini Supersuite|70802|5|Briefly described|250k_pre_mesozoic_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Coompana Province; Madura Province. Events: Maralinga Event (1200-1100 Ma); Albany-Fraser Orogeny Stage II (1225-1140 Ma); Musgrave Orogeny (1220-1150 Ma); Coompana Province events (2500-1200 Ma).|1200-1100 Ma (inferred)||||Dominantly gabbroic rocks; may include leucogabbro, granite, and inclusions of basalt|
79174|Moodini Supersuite|70813|6|Mentioned|p5|||Albany-Fraser Orogen.||||||
79174|Moodini Supersuite|70831|5|Briefly described|p26|Stenian|Stenian|Madura Province.|c. 1192-1130 Ma|||||
79174|Moodini Supersuite|71143|5|Briefly described|p427,429,431,433-438|Stenian|Stenian|Geological province: Madura and Coompana provinces. Contains juvenile isotopic signatures interpreted to reflect mixed mafic lower-crustal and asthenospheric melts produced at the base of thinned crust. Comprises three main magmatic groups; 1192-1150Ma crustal melts (western Coompana Province), 1181-1125 high-KFe mafic to granitic intrusions (Madura Province) and the 1192-1180 Ma Bottle Corner Shoshonite (western Coompana Province). |1192-1125 Ma||Includes Bottle Corner Shoshonite.|||
79174|Moodini Supersuite|71165|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||Bottle Corner Shoshonite, Kestral Cavern Gabbro.|Intrudes Undawidgi Supersuite.|Granitic and gabbroic rocks.|25-JUN-17
79174|Moodini Supersuite|71618|6|Mentioned|p135|Mesoproterozoic|Mesoproterozoic|Geological province: Madura and Coompana provinces. Possible source of c. 1150 (~1000-1300) Ma zircon in Shanes Dam Conglomerate.||||||
79174|Moodini Supersuite|71891|5|Briefly described|p8, p32, p44-p46|||Coompana Province.|||||Equigranular to porphyritic, massive syenogranites, shoshonites and monzogranites.|
79174|Moodini Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Coompana Province; Madura Province.|||||Granitic and gabbroic rocks; typically undeformed.|30-NOV-21
79174|Moodini Supersuite|72059|5|Briefly described|p57|Stenian|Stenian|Geological province: Fraser Zone, Albany-Fraser Orogen. Magmatism associated with Stage II (1225-1140 Ma) Albany-Fraser Orogeny.||||||
79174|Moodini Supersuite|72242|5|Briefly described|p27,29-30|Stenian|Stenian|Geological province: Madura and Musgrave provinces. Bimodal magmatism associated with Maralinga Event (including Musgrave Orogeny). Coeval with Pitjantjatjara Supersuite.|c. 1200-1120||Includes Koonalda Supersuite.|||
79174|Moodini Supersuite|72344|5|Briefly described|p3, p5, p7-p9, p23, p28, p49-p50, p54|Stenian|Stenian|Coompana Province. Intersected in drillhole CDP001 where magmatic crystallisation was dated via SHRIMP at 1141 +/- 15 Ma (present volume). An additional magmatic age of 1148 +/- 7 Ma is derived from this volume via SHRIMP. Petrography, SHRIMP analyses and geochemistry are discussed for several samples. See also p76, p84, p102, p143, p160.|c. 1191-1140 Ma||Includes the Koonalda Suite.||High-K-Mg shoshonitic magmas that are bimodal; includes equigranular to porphyritic, massive syenogranites, shoshonites and monzogranites that form thin sheets.|
79174|Moodini Supersuite|72465|5|Briefly described|p4, 10|||Coompana Province. Crustal thinning and reworking produced widespread intra-plate intrusions. The text also gives an age range of c.1190-1140 Ma.|1168 +/- 6 Ma to 1140 +/- 8 Ma.||||Thin sheets of equigranular to porphyritic, massive syenogranites, shoshonites and monzogranites.|
79174|Moodini Supersuite|72466|5|Briefly described|p4, 10|||Spaggiari and Smithies (2015). Basement to western Coompana Province. Reflects deep melting of wet, oxidised modified mantle lithosphere and widespread reworking of the crust.|1613/- 13 Ma to 1591 +/- 11 Ma.||||Includes equigranular to porphyritic, massive syenogranites, shoshonites and monzogranites that form thin sheets.|
79174|Moodini Supersuite|72467|5|Briefly described|p4, 10, 17|||Coompana Province. Crustal thinning and reworking produced widespread intra-plate intrusions. The text also gives an age range of c.1190-1140 Ma.|1168 +/- 6 Ma to 1140 +/- 8 Ma.||||Thin sheets of equigranular to porphyritic, massive syenogranites, shoshonites and monzogranites.|
79174|Moodini Supersuite|72468|5|Briefly described|p4, p10|Stenian|Stenian|Coompana Province. Represents widespread intraplate magmatism. May represent a MASH zone. Magmatic ages of 1168 +/- 6 Ma and 1140 +/- 8 Ma.|c. 1190-1140 Ma||||Bimodal shoshonitic rocks including equigranular to porphyritic, massive syenogranites, shoshonites and monzogranites.|
79174|Moodini Supersuite|72469|5|Briefly described|p4, p10, p17|Stenian|Stenian|Coompana Province. Represents widespread intraplate magmatism. May represent a MASH zone. Magmatic ages of 1168 +/- 6 Ma and 1140 +/- 8 Ma.|c. 1190-1140 Ma||||Bimodal shoshonitic rocks including equigranular to porphyritic, massive syenogranites, shoshonites and monzogranites.|
79174|Moodini Supersuite|72470|5|Briefly described|p4, p10, p24|Stenian|Stenian|Coompana Province. Represents widespread intraplate magmatism. May represent a MASH zone. Magmatic ages of 1168 +/- 6 Ma and 1140 +/- 8 Ma.|c. 1190-1140 Ma||||Bimodal shoshonitic rocks including equigranular to porphyritic, massive syenogranites, shoshonites and monzogranites.|
79174|Moodini Supersuite|72471|5|Briefly described|p4, p10|Stenian|Stenian|Coompana Province. Represents widespread intraplate magmatism. May represent a MASH zone. Magmatic ages of 1168 +/- 6 Ma and 1140 +/- 8 Ma.|c. 1190-1140 Ma||||Bimodal shoshonitic rocks including equigranular to porphyritic, massive syenogranites, shoshonites and monzogranites.|
79174|Moodini Supersuite|72472|5|Briefly described|p4, p10|Stenian|Stenian|Coompana Province. Represents widespread intraplate magmatism. May represent a MASH zone. Magmatic ages of 1168 +/- 6 Ma and 1140 +/- 8 Ma.|c. 1190-1140 Ma||||Bimodal shoshonitic rocks including equigranular to porphyritic, massive syenogranites, shoshonites and monzogranites.|
79174|Moodini Supersuite|72710|6|Mentioned|p4.|Stenian|Stenian|This supersuite intrudes into both the Coompana and Madura.|1192 Ma to 1127 Ma.||||Includes granitic rocks.|
79174|Moodini Supersuite|72934|5|Briefly described|p2, p4, p11-13, App.A|Stenian|Stenian|Intrude the western part of the Coompana Province. Appears to be part of a much larger crustal reworking event that followed convergence of the South, West and North Australian Cratons. Yielded U-Pb SIMS zircon magmatic crystallisation ages of 1198 +/- 11 Ma, 1174 +/- 9 Ma, 1150 +/- 5 Ma, and 1141 +/- 15 Ma; and inheritance ages of 1527 +/- 6 Ma and 1622 +/- 14 Ma.|1192-1125 Ma||||High-K, Mg shoshonitic mafic to granitic plutons with lesser high-K, Fe A-type rocks.|
79174|Moodini Supersuite|72947|5|Briefly described|p4, p7-9, p14, p16|Stenian|Stenian|Coompana Province. Represents extension and partial melting of the crust. Part of a broader tectonomagmatic event between the West, South and North Australian cratons, affecting the Musgrave Province to the north, and the Madura Province and Albany-Fraser Orogen to the west.|[c.] 1192 - [1150/1141/1140] Ma||Merdayerrah Shoshonite, Koonalda Suite, Albala-Karoo Syenogranite|||29-NOV-22
79174|Moodini Supersuite|73084|4|Described|p: 12, 15, 21, 24, 28, 39, 45, 54, 56...|Stenian|Stenian|Madura and Coompana Provinces. Part of a regionally extensive, high-temperature event named the Maralinga Event by Spaggiari et al. (2016). Compositionally similar and broadly contemporaneous with Pitjantjatjara Supersuite of the Musgrave Province and Esperance Supersuite, particularly Booanya Suite, of the Albany-Fraser Orogen. Dominates much of the Madura Province (intrusions between 1182-1127 Ma). Regionally extensive and slightly older in the Coompana Province (1192-1140 Ma). Report includes lithologic/petrographic description, structural analysis, whole-rock geochemistry, geochronology, Sm-Nd, Lu-Hf. [an informal monzonite from the unit is referred to by a location name; not interpreted to reflect a specific lithologic unit; i.e., Hannah]. Also p: 63, 69-73, 79, 81, 84, 89, ~94-118, ~123-142.|1192-1127 Ma||Kestrel Cavern Gabbro, Bottle Corner Shoshonite, Koonalda Suite||Ferrogabbroic to granitic rocks including shoshonite, granite, pegmatite, mozogranite, granodiorite.|
79174|Moodini Supersuite|73091|5|Briefly described|map legend|Stenian|Stenian||c. 1200-1120 Ma||Includes the Koonalda Suite.||Felsic intrusives.|30-NOV-21
79174|Moodini Supersuite|73224|6|Mentioned|p42, p44|Stenian|Stenian||c. 1181-1125 Ma||Konalda Suite|||
79174|Moodini Supersuite|73225|5|Briefly described|p2, 4, 11, 18|||Madura Province. West of Mulyawarra Shear Zone. Represents low-medium-P melts of mafic crust. Appears as Moodini Suite on p11. Age range also given as c.1192-1175 Ma.|1181-1125 Ma.||Koonalda Suite; Bottle Corner Shoshonite.||High K-Fe rocks; granites.|
79174|Moodini Supersuite|73641|5|Briefly described|p2, 4||||1175-1140 Ma||Koonalda Suite|Is intruded by Giants Head Suite.|Extensive mafic-felsic magmatism.|
80088|Moodogara Dyke Suite|70795|5|Briefly described|2_5m_interpdykel15_lut.csv|Paleoproterozoic|Paleoproterozoic||2208 Ma||||Dolerite.|
80088|Moodogara Dyke Suite|70826|6|Mentioned|p14 tbl 5|Rhyacian|Rhyacian|Hamersley region.|2208 Ma|||||
36888|Moogie Metamorphics|23525|4|Described|p8|Paleoproterozoic|Paleoproterozoic|Previously partly included in "Morrissey Metamorphic Suite"||||||07-NOV-08
36888|Moogie Metamorphics|23527|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Dalgaringa Supersuite, Gascoyne Complex.||||||07-NOV-08
36888|Moogie Metamorphics|23781|4|Described|p61||Paleoproterozoic|Geological Province: Glenburgh Terrane.||||||07-NOV-08
36888|Moogie Metamorphics|24544|4|Described|p5, 38|Paleoproterozoic|Archean|Pelitic and psammitic schist, quartzite, calc-silicate gneiss, marble, amphibolite, ultramafic schist, and metamorphosed banded iron-formation. Unconformably overlain by Mount James Formation. Previously of Morrissey Metamorphic Suite.||||||07-NOV-08
36888|Moogie Metamorphics|50216|5|Briefly described|p205|Paleoproterozoic|Paleoproterozoic|Calc-silicate gneiss, amphibolite and pelitic metasedimentary rocks. Geological Province: Glenburgh Terrane (Gascoyne Complex).||||||07-NOV-08
36888|Moogie Metamorphics|50218|5|Briefly described|p240 Fig.2, p242|||Includes the Mumba Pelite. Geological Province: Glenburgh Terrane (Gascoyne Complex). See also p245.||||||07-FEB-11
36888|Moogie Metamorphics|50219|5|Briefly described|p259, p260 Fig. 2|Paleoproterozoic|Paleoproterozoic|Interleaved with rocks of Dalgaringa Supersuite.  Metasedimentary rocks.  Includes Mumba Pelite.  Geological Province: Glenburgh Terrane (Gascoyne Complex).||||||07-FEB-11
36888|Moogie Metamorphics|50226|5|Briefly described|p418|Paleoproterozoic|Paleoproterozoic|Of the Gascoyne Complex (Glenburgh Terrane).  Metasedimentary rocks.||||||07-NOV-08
36888|Moogie Metamorphics|61262|5|Briefly described|p454|Paleoproterozoic|Paleoproterozoic|Part of Morrissey Metamorphic Suite. Age: >2000Ma. ||||||07-NOV-08
36888|Moogie Metamorphics|63246|5|Briefly described|p480 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: >2000Ma. In the Gascoyne Complex.||||||07-NOV-08
36888|Moogie Metamorphics|63866|5|Briefly described|p155-p156, p177||||>2005 Ma (inferred, unit relationship)|||Intruded by the Bertibubba Supersuite and Dalgaringa Supersuite.|Calc-silicate gneiss, amphibolite and pelitic metasedimentary rocks.|
36888|Moogie Metamorphics|63869|6|Mentioned|p17|||Southern Gascoyne Complex. Sedimentary protoliths deposited >2005 Ma (Occhipinti and Sheppard, 2001).||||||
36888|Moogie Metamorphics|64580|4|Described|map legend||Paleoproterozoic|Pelite, quartzite, marble and calc-silicate gneiss, and amphibolite.||||||15-DEC-08
36888|Moogie Metamorphics|65152|5|Briefly described|p1.|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane. Psammites and pelites <2000 Ma, unconformably overlying Halfway Gneiss. Includes relict pelitic migmatites, now pervasively retrogressed to chloritoid-bearing schists.||||||01-MAY-15
36888|Moogie Metamorphics|65450|6|Mentioned|p2 Fig.1|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.||||||
36888|Moogie Metamorphics|65830|6|Mentioned|p24, p26 Fig.13, p28|Orosirian||Older than the Dalgaringa Supersuite which intrudes the Moogie Metamorphics between 2005-1970 Ma.|> 2005 Ma (Occhipinti and Sheppard, 2001).|||Intruded by the Dalgaringa Supersuite.|Metasedimentary rocks.|
36888|Moogie Metamorphics|66105|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, Gascoyne Province. 2240-2125 Ma. Calc-silicate gneiss; pargasite- or diopside-bearing quartz-plagioclase-epidote(-titanite) rock; tremolite-diopside(-garnet) calc-silicate rock with minor marble.||||||
36888|Moogie Metamorphics|66110|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, Gascoyne Province. Includes pelitic schists, metamorphosed siliciclastics, calc-silicate gneiss, and the Mumba Psammite.||||||
36888|Moogie Metamorphics|66299|4|Described|pp3-5, pp57-59, pp66-72.|Paleoproterozoic|Paleoproterozoic|Component of Glenburgh Terrane, basement to Gascoyne Province. Psammitic and pelitic rocks interfolded with Halfway Gneiss. Rafts of calc-silicate gneiss occur in Nardoo Granite. |Deposition 2240-2125 Ma. Metamorphosed c.1770 Ma.||Includes Mumba Psammite.|Interleaved with Halfway Gneiss and a unit of Moorarie Supersuite. Intruded by Dalgaringa Supersuite.|Psammitic and pelitic schists; calc-silicate rock; minor quartzite, marble, amphibolites and ultramafic schist.|
36888|Moogie Metamorphics|66574|6|Mentioned|p928|Orosirian|Neoarchean|Gascoyne Province.  Deposited between 2610-1965 Ma in either a foreland or retroarc tectonic setting, during collision of the Glenburgh Terrane with the Pilbara Craton.||||||
36888|Moogie Metamorphics|66579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, Gascoyne Province.|||Includes Mumba Psammite and two unnamed units.||Pelitic schist, quartzofeldspathic psammite schist, quartzite, metaconglomerate, gneiss.|
36888|Moogie Metamorphics|66887|4|Described|p1, p3 Fig.2, p5 Fig.4, p6, p7, p21|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, southern Gascoyne Province. Max age: youngest detrital zircons (Mumba Psammite) age indicates protoliths of parent (Moogie Metamorphics) were deposited after c. 2240 Ma (Johnson et al. 2010). Suggested min age of deposition is c. 2125 Ma (metamorphic zircons and monazites in Mumba Psammite. Johnson et al. 2010).|max  c. 2240 Ma; min deposition c. 2125 Ma||Mumba Psammite|In tectonic contact with, and locally unconformably overlies, Halfway Gneiss. Interleaved with mesocratic Halfway Gneiss on both sides of Ti Tree Shear Zone.|Package of continent-derived siliciclastic metasedimentary rocks, dominated by psammitic schist (Mumba Psammite), but also includes pelitic schist, quartzite, calc-silicate, and marble.|14-DEC-16
36888|Moogie Metamorphics|66950|5|Briefly described|p7, p9 Fig.8, p10 Fig.9, p18|Rhyacian|Rhyacian|Includes rocks reassigned from the invalid Morrissey Metamorphics, including type areas from the original "Morrissey Metamorphic Suite" (Williams et al. 1978). Displays evidence of retrogression as garnet porphyroblasts are pseudomorphed by chloritoid, and sillimanite is replaced by sericite.|c. 2240-2125 Ma|||Intruded by the Dalgaringa Supersuite. Unconformably underlain by the Halfway Gneiss.|Comprises garnet-silimanite pelitic and semi-pelitic schists.|16-DEC-16
36888|Moogie Metamorphics|67201|6|Mentioned|p35 Fig.19|||||||||
36888|Moogie Metamorphics|67247|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, Gascoyne Province.|||||Pelitic schist, commonly with chloritoid; locally with relict garnet porphyroblasts.|
36888|Moogie Metamorphics|67346|6|Mentioned|p794 Fig.1|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.||||||11-MAY-12
36888|Moogie Metamorphics|67371|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, Gascoyne Province.|||Includes Mumba Psammite and two un-named members, mapped separately.||Quartzofeldspathic psammitic schist commonly with chloritoid; local minor pelitic schist and quartzite; metamorphosed quartz sandstone and granule metaconglomerate; pelitic schist; calc-silicate gneiss; marble; dolomite; serpentinite.|
36888|Moogie Metamorphics|67373|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, Gascoyne Province. |||Includes Mumba Psammite.||Psammitic schist, calc-silicate gneiss, marble.|
36888|Moogie Metamorphics|67843|3|Fully described|Throughout the article.|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane. Outcrops as discrete packages of siliciclastic metasedimentary rocks whose precursors were deposited between 2240 and 2125 Ma. Derived from underlying Halfway Gneiss. Upper amphibolite facies metamorphism, with widespread production of garnet, ?staurolite and sillimanite porphyroblasts and migmatitic textures.|2240-2125 Ma.||Includes Mumba Psammite.|Unconformably overlies Halfway Gneiss. Is intruded by Dalgaringa Supersuite. Is intercalated with Halfway Gneiss.|Retrogressed pelitic diatexites and schists, psammitic schists with minor calc-silicate gneiss, quartzite, dolomitic marble and amphibolite.|
36888|Moogie Metamorphics|68521|5|Briefly described|Map Legend||Siderian||< c.2300 Ma||Includes Mumba Psammite.||Schists, gneiss, metasandstone, marble or calc-silicate rock, amphibolite.|
36888|Moogie Metamorphics|68522|5|Briefly described|Map Legend|Rhyacian|Rhyacian|Gascoyne Province. |2240-2125 Ma||Includes Mumba Psammite.||Marble, dolomite rock; calc-silicate gneiss; pelitic schist; quartzofeldspathic psammitic schist; metamorphosed quartz sandstone, granule metaconglomerate, quartzite gneiss.|
36888|Moogie Metamorphics|69003|4|Described|p4, p7-9, p10 Figs.10-11|||Glenburgh Terrane. Pro-foreland basin deposits from the eroded Ophthalmia Fold Belt. Sediments sourced from Halfway Gneiss.|2240 - 2125 Ma.|||Unconformably overlies, and is in tectonic contact with, Halfway Gneiss.|Strongly deformed and metamorphosed psammitic metasedimentary rocks.|
36888|Moogie Metamorphics|69011|5|Briefly described|Map Legend|Rhyacian|Rhyacian|Glenburgh Terrane, Gascoyne Province.|2240-2125 Ma||Includes the Mamba Psammite.||Includes metamorphosed quartz sandstone, granule metaconglomerate, and quartzite gneiss, locally micaceous; minor psammitic scdhist; locally with relict cross-bedding.|
36888|Moogie Metamorphics|69028|5|Briefly described|Map Legend|Rhyacian|Rhyacian|Glenburgh Terrane, Gascoyne Province.|2240-2125 Ma||||Psammitic and pelitic schist; calc-silicate rock; minor quartzite, marble, amphibolite, and ultramafic schist.|06-MAY-14
36888|Moogie Metamorphics|69080|5|Briefly described|p684, p688-689, p689|||Gascoyne Province. Glenburgh Terrane. Protoliths deposited coincident with the 2215-2145 Ma Ophthalmian Orogeny. Contains detrital zircons from southern Pilbara region.||||Coeval with Beasley River Quartzite.|Psammitic and pelitic schist; calc-silicate rock; minor quartzite, marble, amphibolites, and ultramafic schist.|
36888|Moogie Metamorphics|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Age derived from quartzite sample (190651.1.pdf) and constrains the maximum age of sandstone protolith.|2295 Ma +/- 11 Ma (SHRIMP)||Includes Mumba Psammite|Unconformably overlain by Halfway Gneiss|Marble; dolomite, calc-silicate gneiss; pargasite or diopside bearing quartz-plagioclase-epidote rock; tremolite-diopside calc-silicate rock with minor marble.|
36888|Moogie Metamorphics|69237|6|Mentioned|p2|||Gascoyne Province.||||||
36888|Moogie Metamorphics|69387|5|Briefly described|p3,p6,p14-16,p18,p22-23,p25,p37,p48|Rhyacian|Rhyacian|Glenburgh Terrane, Gascoyne Province. Deformations discussed. SG and magnetic susceptibility values given. Gravity and magnetic modelling. Hosts W-rich mineralisation at Hectors Bore.|c.2240-2125 Ma.|||Overlies Halfway Gneiss. Is intruded by Dalgaringa Supersuite.|Siliciclastic metasedimentary rocks, marble.|
36888|Moogie Metamorphics|69546|6|Mentioned|p102|||Geological province: Gascoyne Province.||||||
36888|Moogie Metamorphics|69583|5|Briefly described|p130-132, p137, Plate 3|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Probably time-equivalent to the Beasley River Quartzite. Age range also given as c.2240-2125 Ma.|c.2240-2145 Ma (protolith deposition).|||Overlies Halfway Gneiss.|Continent-derived siliciclastic metasedimentary rocks. Psammitic and pelitic schists, calc-silicate rock; minor quartzite, marble, amphibolites and ultramafic schist.|
36888|Moogie Metamorphics|69596|5|Briefly described|p5, p8|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|c.2240-2125 Ma (protolith deposition).|||Overlies the Halfway Gneiss. Is intruded by Dalgaringa Supersuite.|Siliciclastic metasedimentary rocks.|
36888|Moogie Metamorphics|70019|5|Briefly described|p94|Rhyacian|Rhyacian|Geological province: Gascoyne Province, Capricorn Orogen. Comprises Neoarchean to Paleoproterozoic basement rock assemblage of the Gascoyne Province. Package of medium- to high-grade metasedimentary rocks.|2240-2145 Ma|||||
36888|Moogie Metamorphics|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 2_5m_interpgeop15_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeol_lut.csv, 208331.1.pdf,  West Australian Craton, Bryah Basin|2240-2125 Ma||Includes Mumba Psammite|Intruded by Moorarie Supersuite|Marble, dolomite, dolomite-calcite-forsterite-clinohumite-serpentine rock. Calc-silicate gneiss; pargasite or diopside quartz-plagioclase-epidote rock. Psammitic and pelitic schist; minor quartzite, marble, amphibolites and ultramafic schist.|
36888|Moogie Metamorphics|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|Probably a time equivalent to the Shingle Creek Group. Glenburgh Terrane, Gascoyne Province.||||||
36888|Moogie Metamorphics|71000|6|Mentioned|p64-65, 79-80|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, southern Gascoyne Province, Capricorn Orogen.|2240-2145 Ma; protolith deposition.|||Unconformably and tectonically overlies Halfway Gneiss. Faulted against (in tectonic contact with) Camel Hills Metamorphics.||
36888|Moogie Metamorphics|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||pelite, felsic schist, quartzite, calc-silicate rock|
36888|Moogie Metamorphics|71869|6|Mentioned|p4|||Emplaced during the Ophthalmia Orogeny.||||||
36888|Moogie Metamorphics|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, Capricorn Orogen.|Max age 2240 +/-8 Ma, min 2125+/-5 Ma.||||Psammitic and pelitic schist; calc-silicate rock; minor quartzite, marble, amphibolites, and ultramafic schist.|
36888|Moogie Metamorphics|72259|6|Mentioned|p3-4, p6, App. Fig.S5, App. Tb.B|Rhyacian|Rhyacian||ca. 2240-2125 Ma||||Includes metasedimentary rocks (quartzite, psammite, pelite) and quartzofeldspathic migmatite.|
36888|Moogie Metamorphics|73102|5|Briefly described|p3|||Gascoyne Province; Glenburgh Terrane.|||||Psammitic and pelitic/schist; calc-silicate rock; minor quartzite, marble, amphibolites, and ultramafic schist.|
36888|Moogie Metamorphics|73168|5|Briefly described|p758, 764-765|Rhyacian|Rhyacian|Gascoyne Province. Glenburgh Terrane. Contains detrital zircon ages of late Neoarchean (ca 2850-2700 Ma) and early Paleoproterozoic (ca 2550-2300), recycled from Fortescue and Hamersely groups. Includes 3300-2900 Ma detrital zircon ages interpreted to come from Halfway Gneiss basement and the Pilbara Craton. Protoliths were deposited between 2240 and 2145 Ma in a foreland basin, after emplacement of the Halfway Gneiss protoliths.|2240-2145 Ma|||Interleaved with Halfway Gneiss.|Interleaved calc-silicate, amphibole and pelitic gneiss.|
36888|Moogie Metamorphics|73214|6|Mentioned|p974 Fig.1|Palaeoproterozoic||Glenburgh Terrane.||||||
36888|Moogie Metamorphics|73442|5|Briefly described|p3|||Gascoyne Province, Glenburgh Terrane.|||||Psammitic and pelitic schist; calc-silicate rock; minor quartzite, marble, amphibolites, and ultramafic schist.|
67859|Mooline Formation|24544|5|Briefly described|p48|Paleoproterozoic|Paleoproterozoic|Of Capricorn Group. Geological Province: Ashburton Province.||||||07-NOV-08
67859|Mooline Formation|63866|5|Briefly described|p154, p175|Statherian|Orosirian|Blair Basin. |1801 +/- 14 Ma (GSWA, 148925)|Capricorn Group||Overlies the Bywash Formation.|Coarse-grained lithic sandstone.|
67859|Mooline Formation|63869|4|Described|p7-9, Plate 1|Paleoproterozoic|Paleoproterozoic|Named after Mooline Well on central CAPRICORN sheet. Maximum age from detrital zircons. Thickness estimated at 1.1 km to 2.5 km. Lithology described in some detail.|<1801 +/- 14 Ma (SHRIMP U-Pb; GSWA, 2005).|Upper unit in Capricorn Group.||Conformably overlies Bywash Formation.|Thin- to very thick-bedded sandstone, dolomitic sandstone, siltstone, dolostone, conglomerate and minor felsic volcaniclastic sandstone.|
67859|Mooline Formation|65830|6|Mentioned|Plate 2|Statherian|Orosirian|Blair Basin.||Unit in Capricorn Group.||||
67859|Mooline Formation|69024|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Blair Basin. Includes 3 unnamed subunits mapped separately: see legend for lithologies..||Of the Capricorn Group.||Overlies Bywash Formation.|Undivided: fine to very coarse grained sandstone, siltstone, conglomerate, dolostone, dolomitic siltstone, and felsic volcaniclastic sandstone.|05-MAY-14
67859|Mooline Formation|69028|5|Briefly described|Map Legend|Orosirian|Orosirian|Ashburton and Blair Basins. Mapped with Bywash Formation as a single unit.|c. 1805 Ma|Of the Capricorn Group.|||Conglomerate, ferruginous and quartzitic sandstone, ferruginous siltstone and mudstone, dolostone, and felsic volcanic rock.|07-MAY-14
67859|Mooline Formation|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Age derived from lithic sandstone sample (148925.1.pdf)|1801 Ma +/- 14 Ma (SHRIMP)|Capricorn Group|||Laminated felsic volcaniclastic rock, and accretionary lapilli tuff. Siltstone, conglomerate, pebbly sandstone, fine-very coarse grained sandstone, dolostone, dolomitic siltstone and sandstone, and felsic volcaniclastic sandstone.|
67859|Mooline Formation|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_interpgeop_lut.csv, 148925.1.pdf|1801-1738 Ma|Capricorn Group|||Fine to very coarse grained sandstone, siltstone, polymictic, clast and matrix supported conglomerates, dolostone, dolomitic siltstone, lithic sandstone and quartz sandstone.|
67859|Mooline Formation|70814|6|Mentioned|p73|||||Capricorn Group||||
67859|Mooline Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone, conglomerate, crystalline dolostone/dolomite|
67859|Mooline Formation|72259|6|Mentioned|p3|Orosirian|Orosirian||ca. 1805 Ma|||||
22371|Mooloogool Group|23586|5|Briefly described|p15|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
22371|Mooloogool Group|24535|5|Briefly described|p22, 23|Paleoproterozoic|Paleoproterozoic|Siliciclatic sedimentary andmafic igneous rocks. Overlies Windplain Group. Geological Province: Yerrida Basin.|||Includes Doolgunna, Thaduna, Killara and Maraloou Formations.|||26-NOV-13
22371|Mooloogool Group|50195|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes the Killara Formation.  Geological Province: Yerrida Basin.||||||07-NOV-08
22371|Mooloogool Group|50222|4|Described|p322|Paleoproterozoic|Paleoproterozoic|Supersedes the Mooloogool Subgroup.  Overlies the Windplain Group.  Includes the Thaduna, Doolgunna, Killara and Maraloou Formations; incorporates fragments of Narracoota Fm (of the Bryah Group).  Geological Province: Yerrida Basin.  See also p319 Fig. 2||||||07-NOV-08
22371|Mooloogool Group|50226|5|Briefly described|p420, p421 Fig. 4|Paleoproterozoic|Paleoproterozoic|Unconformably overlain by Earaheedy Group.  Age: 1.84Ga.  Geological Province: Yerrida Basin.  See also p423.||||||07-NOV-08
22371|Mooloogool Group|62094|5|Briefly described|p236|||Includes the Killara Formation. Geological Province: Yerrida Basin.||||||21-FEB-07
22371|Mooloogool Group|63866|5|Briefly described|p152, p166, p168, p175|||Yerrida Basin.||||Overlain by the Eraheedy Group.||
22371|Mooloogool Group|64580|6|Mentioned|map legend|||||||||
22371|Mooloogool Group|64772|5|Briefly described|p8, p9, Plate 1, p19 Fig.9|Paleoproterozoic|Paleoproterozoic|Includes Killara and Maraloou Formations. Age: c. 1840Ma. Geological province: Yerrida Basin.||||||25-NOV-13
22371|Mooloogool Group|65472|5|Briefly described|p1, p2, p3 Fig.2, p8 Fig.7, p16|||Yerrida Basin.|c. 1.84 Ga||Includes Thaduna Formation, Doolgunna Formation, Killara Formation, Maraloou Formation|Unconformably overlain by Earaheedy Group; overlies Windplain Group (contact poorly defined, but where exposed is discomformable).||24-SEP-15
22371|Mooloogool Group|66427|5|Briefly described|p42, p47-48, p52, p74  |||Yerrida Basin. Eruptions accompanying an uplift and rifting event at 1.84 Ga.||||Unconformably underlies the Earaheedy Group.|Flood basalts.|
22371|Mooloogool Group|68055|6|Mentioned|p77-78|||Yerrida Basin. Source of some sediments for Yelma Formation.|||Maraloou Formation.|||
22371|Mooloogool Group|68471|6|Mentioned|p17|||Yerrida Basin rift phase.|>1.84 Ga.|||||
22371|Mooloogool Group|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic||||Includes Doolgunna Formation, Killara Formation, Maraloou Formation, Thaduna Formation.|||
22371|Mooloogool Group|69003|5|Briefly described|p4, p10-13, p26|Paleoproterozoic|Paleoproterozoic|Yerrida Basin, Capricorn Orogen. Separated from the underlying unit by a 300-400 m.y. hiatus.|||Maraloou, Killara, Doolgunna, Thaduna Formations.|Disconformably overlies Windplain Group.||
22371|Mooloogool Group|69152|6|Mentioned|GEOL_LUT_CSV files + geochron files||||||Includes Killara Formation, Doolgunna Formation, Maraloou Formation, Thaduna Formation.|||06-AUG-15
22371|Mooloogool Group|69166|6|Mentioned|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||Includes Doolgunna Formation, Thaduna Formation|||
22371|Mooloogool Group|69313|5|Briefly described|p21, p92|||Represents a rifting event that began at ~1.84 Ga.|||||Flood basalts.|08-SEP-17
22371|Mooloogool Group|69596|5|Briefly described|p4, p9-10, p32-34|Paleoproterozoic|Paleoproterozoic|Yerrida Basin, Capricorn Orogen. The basal disconformity represents a c.330 m.y. hiatus. Conductivity discussed.|||Killara, Doolgunna, Thaduna, Maralou Formations.|Disconformably overlies Windplain Group.||
22371|Mooloogool Group|70136|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Yerrida Basin.|||Thaduna Formation.|||
22371|Mooloogool Group|70153|5|Briefly described|100k_geologyp10_lut.csv|Paleoproterozoic|Paleoproterozoic|Also known as Mooloogool Subgroup.|||Includes Maraloou Formation, Doolgunna Formation, Thaduna Formation.|||
22371|Mooloogool Group|70795|5|Briefly described|2_5m_interpgeop15_lut.csv|Paleoproterozoic|Paleoproterozoic|West Australian Craton|2170-1600 Ma||||Sandstone overlain by mafic volcanic rocks and fine grained siliciclastic rocks.|
22371|Mooloogool Group|70796|4|Described|2_5m_interpgeop15_lut.csv|Paleoproterozoic|Paleoproterozoic|Of the Yerrida Basin, Capricorn Orogen. See also 500k_interpgeop14_lut.csv.|ca 2170 1600 Ma (inferred)||Includes the Maraloou Formation, Killara Formation, Doolgunna Formation, Thaduna Formation.||Sandstone overlain by mafic volcanic rocks and finegrained siliciclastic rocks.|
22371|Mooloogool Group|70826|6|Mentioned|p6 tbl 2, p9|Paleoproterozoic|Paleoproterozoic|Yerrida Basin.||||Overlies the Windplain Group. Overlain by the Bryah and Padbury Groups.||
22371|Mooloogool Group|71269|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Of Yerrida Basin. Events: Capricorn Orogeny (1817-1772 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv, glengarry_100k_geologyp_lut.csv.|2170-1600 Ma (inferred)||Includes Doolgunna Formation, Killara Formation, Maraloou Formation, Thaduna Formation.||Sandstone overlain by mafic volcanic rocks and fine-grained siliciclastic rocks|
22371|Mooloogool Group|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen. Of Earaheedy Basin. Events: Capricorn Orogeny (1817 - 1772 Ma). See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 100k_geologysub10_lut.csv, 2_5m_interpgeop15_lut.csv.|2170-1600 Ma (inferred)||Includes Doolgunna Formation, Killara Formation, Thaduna Formation.||Sandstone overlain by mafic volcanic rocks and fine-grained siliciclastic rocks|
22371|Mooloogool Group|71468|4|Described|p26|Orosirian|Orosirian|Geological province: Capricorn Orogen, Yilgarn Craton. Of Yerrida Basin. Minimum depositional age is c. 1990 Ma (1990+\-6 Ma at base of overlying Tooloo Group; Nelson, 2001; Pirajno et al., 2009; Sheppard et al., 2016). Max depositional age constrained by underlying Juderina Formation (maximum depositional age of c. 2180 Ma; Nelson 2002). Age is loosely bracketed between c. 2180 and 1990 Ma.|||Includes Maraloou, Doolgunna, Thaduna and Killara formations.|Overlain by Tooloo Group. Underlain by Juderina Formation.||
22371|Mooloogool Group|71484|5|Briefly described|p122-125,128,130,134,139|||Geological province: Of Yerrida Basin. Outcrops in the central part of the Yerrida Basin, above the Windplain Group.|||Includes Maraloou, Doolgunna, Thaduna and Killara formations.|Overlain unconformably by Tooloo Group.||30-AUG-19
22371|Mooloogool Group|72034|6|Mentioned|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Maraloou Formation, Killara Formation, Doolgunna Formation, Thaduna Formation.|||
38010|Moolyella Monzogranite|24025|5|Briefly described|p60, p11 Tb. 2|Archean|Archean|Of Mount Edgar Granitoid Complex.  Geological Province: Pilbara Craton.||||||07-NOV-08
38010|Moolyella Monzogranite|24110|5|Briefly described|Plate 1|Archean|Archean|Belongs to Mount Edgar Granitoid Complex. Geological Province: Pilbara Craton.||||||19-MAR-13
38010|Moolyella Monzogranite|24193|5|Briefly described|p874, p875 Fig.2, p877 Tb.1|Archean|Archean|Of Mount Edgar granitoid complex. Geological Province: Pilbara Craton.||||||07-NOV-08
38010|Moolyella Monzogranite|50427|5|Briefly described|p193|Archean|Archean|Age: c.2830 Ma. Of Mount Edgar Granitoid Complex.||||||07-NOV-08
38010|Moolyella Monzogranite|63417|5|Briefly described|Map legend|Archean|Archean|Of Split Rock Supersuite. Geological Province: Pilbara Craton. Muscovite-biotite monzogranite, medium-grained, massive to weakly foliated.||||||07-NOV-08
38010|Moolyella Monzogranite|63441|5|Briefly described|p12 tb. 2|Archean|Archean|Of Split Rock Supersuite. Superseded Moolyella Adamellite. Age: 2831+/-11Ma. Geological province: Pilbara Craton.||||||07-FEB-11
38010|Moolyella Monzogranite|64580|4|Described|map legend||Mesoarchean|Of Split Rock Supersuite. Muscovite-biotite monzogranite; medium grained; massive to weakly foliated.||||||15-DEC-08
38010|Moolyella Monzogranite|64621|5|Briefly described|Map legend|Archean|Archean|Of Split Rock Supersuite. Muscovite-biotite monzogranite, medium-grained, massive to weakly foliated; also pegmatite of mainly quartz, albite, microcline, biotite and muscovite.||||||07-NOV-08
38010|Moolyella Monzogranite|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.|c.2831 Ma (Wyatt et al. 2001).|Of Mount Edgar Granitoid Complex.|||Muscovite-biotite monzogranite, medium-grained, massive to weakly foliated.|
38010|Moolyella Monzogranite|65727|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Pilbara Craton. In Version 1 of this map sheet, this unit was part of the Mount Edgar Granitoid Complex.|c.2831 Ma.|Of Split Rock Supersuite. |||Muscovite-biotite monzogranite, medium-grained, massive to weakly foliated.|
38010|Moolyella Monzogranite|65827|3|Fully described|p1; p6,12,14 Tbs.2,3,4; p16; p29; p32|Mesoarchean|Mesoarchean|Of Split Rock Supersuite. Formerly known as Moolyella Granite (de Laeter and Blockley 1972), Moolyella Adamellite (Hickman and Lipple 1975), Moolyella Suite (Collins 1983, 1993). At 2831+/-12 Ma (SHRIMP U-Pb zircon; Nelson 2005), intruded Bishop Creek Monzogranite and Fig Tree Gneiss in the core of the Mount Edgar Granitic Complex. Compositionally similar to Mondana Monzogranite. Post-tectonic. Nonfoliated, massive, medium-grained, grey muscovite-biotite monzogranite. I-A type.||||||
38010|Moolyella Monzogranite|66108|5|Briefly described|Map legend|Neoarchean|Neoarchean|Unit in Split Rock Supersuite. c. 2831 Ma. Muscovite-biotite monzogranite; medium-grained; massive to weakly foliated.||||||15-APR-13
38010|Moolyella Monzogranite|66217|5|Briefly described|p11.|||Undeformed. Sn-Ta mineralisation in pegmatites associated with this unit.||Unit in Split Rock Supersuite.||||
38010|Moolyella Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|Alternatively called Moolyella Adamellite. Age derived from monzogranite samples (142977.1.pdf, 169044.1.pdf)|3240  +/- 11 Ma - 2831 +/- 12 Ma (SHRIMP) |Split Rock Supersuite||Intrudes Johansen Monzogranite|Muscovite--biotite monzogranite; medium grained; massive to weakly foliated. Quartz-albite-microcline-biotite-muscovite pegmatite.|
38010|Moolyella Monzogranite|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Split Rock Supersuite.|||Muscovite-biotite monzogranite; medium grained; massive to weakly foliated|
38010|Moolyella Monzogranite|69590|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Also known as Moolyella Adamellite (Hickman 1983). Events: Pilbara Craton breakup; Split Rock Supersuite Event. Sample GSWA 142977 (monzogranite) yielded a preferred interpreted maximum igneous crystallisation age of 3240+\-11 Ma of the host monzogranite (weighted mean 207Pb/206Pb), or potentially an interpreted igneous crystallisation age of 3313+\-3 Ma (weighted mean 207Pb/206Pb). Sample GSWA 169044 (ms-bt monzogranite) yielded an interpreted igneous crystallisation age of 2831+\-12 Ma for the monzogranite (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|2831 Ma (isotopic)|Unit of Split Rock Supersuite.||Intrudes into Johansen Monzogranite.|Muscovite-biotite monzogranite; medium grained; massive to weakly foliated; pegmatite; mainly composed of quartz, albite, microcline, biotite, and muscovite; locally contains cassiterite, tantalite, beryl, and zinnwaldite.|
38010|Moolyella Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, pegmatite|
38010|Moolyella Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||2831+/-11 Ma|Split Rock Supersuite|||Muscovite--biotite monzogranite; medium grained; massive to weakly foliated.|
25260|Moonlight Valley Tillite|14019|5|Briefly described|p19|Neoproterozoic|Neoproterozoic|Possibly equivalent to diamictite of Duerdin Group. Age: 793 +/- 30Ma (Rb-Sr) and 610Ma. Geological Province: Wolfe Creek Basin. Correlated with Elatina Formation.||||||
25260|Moonlight Valley Tillite|22496|3|Fully described|p11||Neoproterozoic|Of the Duerdin Group. Unconformably overlies both the Illjarra Sandstone and the Eliot Range Dolomite. Geological Province: Wolfe Basin.||||||14-APR-08
25260|Moonlight Valley Tillite|22547|4|Described|p28||Neoproterozoic III|Of the Duerdin Group.  In the  Wolfe Creek Basin. Max. thickness: 280 m. Overlain by Ranford Formation.||||||07-NOV-06
25260|Moonlight Valley Tillite|22901|6|Mentioned|76 fig 2|||||||||
25260|Moonlight Valley Tillite|23314|5|Briefly described|332|||||||||
25260|Moonlight Valley Tillite|23621|4|Described|p33|||See also page 9 Table 1 - Moonlight Vally Tillite (misspelt). Of Duerdin Group. Underlain by Eliot Range Dolomite. Geological Province: Wolfe Basin.||||||09-AUG-06
25260|Moonlight Valley Tillite|23622|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Duerdin Group. Geological Province: Wolfe Basin.||||||
25260|Moonlight Valley Tillite|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|Of Duerdin Group.||||||
25260|Moonlight Valley Tillite|24173|4|Described|p25, p11 Tb.2|Neoproterozoic III|Neoproterozoic III|Of the Duerdin Group. Conformably overlain by Ranford Formation;  unconformable on Eliot Range Dolomite and Illjara Sandstone. Geological Province: Wolfe Basin. Max Thickness: 200m. Correlates with Landrigan Tillite (Kuniandi Group) to the west.||||||06-APR-05
25260|Moonlight Valley Tillite|28255|3|Fully described|p73, Tb.11 (opp. p8)|Adelaidean|Adelaidean|Of the Duerdin Group. Unconformably overlies rocks of the Auvergne Group (AUVERGNE sheet); conformably overlain by Ranford Formation and unconformably overlain in several areas by Kinevans Sandstone and Antrim Plateau Volcanics. Max. thickness: >50m.||||||09-AUG-06
25260|Moonlight Valley Tillite|30533|6|Mentioned|p21|||Correlated with Mount House Group||||||
25260|Moonlight Valley Tillite|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
25260|Moonlight Valley Tillite|32660|5|Briefly described|Table 5|||||||||
25260|Moonlight Valley Tillite|32664|6|Mentioned|Map legend|Adelaidean|Adelaidean|Mention in notes||||||
25260|Moonlight Valley Tillite|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Duerdin Group.  Tillite overlain by dolomite.  sandstone, granitic clasts predominate.||||||02-DEC-04
25260|Moonlight Valley Tillite|32701|4|Described|Table 1|||Adelaidean. Of the Duerdin Group.||||||07-NOV-06
25260|Moonlight Valley Tillite|32720|6|Mentioned|p7|||Age: 739 + or - 30 my.||||||09-AUG-06
25260|Moonlight Valley Tillite|32728|6|Mentioned|Table 7|||See also Fig.16||||||
25260|Moonlight Valley Tillite|33375|6|Mentioned|p11 Tb. 1, p13|Adelaidean|Adelaidean|Of the Duerdin Group. Tillite; cobbles and boulders of quartzite, granite, dolomite, etc; laminated dolomite at top. Conformable on Blackfellow Creek Sandstone; unconformable on Angalarri Siltstone and Saddle Creek Formation.||||||27-APR-05
25260|Moonlight Valley Tillite|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
25260|Moonlight Valley Tillite|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Duerdin Group.  Tillite, laminated dolomite at top.||||||27-APR-05
25260|Moonlight Valley Tillite|34230|6|Mentioned|Plate 8|Proterozoic|Proterozoic|||||||28-OCT-04
25260|Moonlight Valley Tillite|35255|6|Mentioned|p15|||||||||
25260|Moonlight Valley Tillite|36048|6|Mentioned|p377|||||||||
25260|Moonlight Valley Tillite|36551|6|Mentioned|Table 12|||||||||
25260|Moonlight Valley Tillite|36888|4|Described|p215|||||||||
25260|Moonlight Valley Tillite|36898|6|Mentioned|p181|||||||||
25260|Moonlight Valley Tillite|37238|6|Mentioned|p355|||||||||
25260|Moonlight Valley Tillite|37462|5|Briefly described|p293|||||||||
25260|Moonlight Valley Tillite|37927|4|Described|p504|||||||||
25260|Moonlight Valley Tillite|38157|6|Mentioned|Table X|||||||||
25260|Moonlight Valley Tillite|38350|6|Mentioned|p22|||||||||
25260|Moonlight Valley Tillite|38988|6|Mentioned|Fig.4|||||||||
25260|Moonlight Valley Tillite|39210|5|Briefly described|p49|||Age||||||
25260|Moonlight Valley Tillite|39827|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
25260|Moonlight Valley Tillite|40494|4|Described|p11|||||||||
25260|Moonlight Valley Tillite|41405|5|Briefly described|p206|||||||||
25260|Moonlight Valley Tillite|41429|6|Mentioned|p247|||||||||
25260|Moonlight Valley Tillite|42811|5|Briefly described|p30|||||||||
25260|Moonlight Valley Tillite|42829|5|Briefly described|p147|||||||||
25260|Moonlight Valley Tillite|43299|5|Briefly described|Map Legend||Neoproterozoic|Of Duerdin Group.||||||09-AUG-06
25260|Moonlight Valley Tillite|43303|5|Briefly described|Map Legend||Neoproterozoic|Of Duerdin Group.||||||09-AUG-06
25260|Moonlight Valley Tillite|43853|5|Briefly described|Map Legend||Proterozoic|||||||
25260|Moonlight Valley Tillite|43855|5|Briefly described|Map Legend||Proterozoic|||||||
25260|Moonlight Valley Tillite|44140|5|Briefly described|p300, p301 fig 4-7, p302 Tb.4-2|Neoproterozoic|Neoproterozoic|Of East Kimberley area. Up to 140 m thick. Correlated with Marinoan glaciation (670 Ma).||Duerdin Group||Overlies Frank River Sandstone unconformably. Is overlain by Jarrad Sandstone Member (Ranford Formation).|Tillite, lenses of dolomitic quartz sandstone and conglomerate; capped by pink and cream dolomite.|07-MAR-18
25260|Moonlight Valley Tillite|44230|5|Briefly described|Map Legend||Proterozoic|||||||
25260|Moonlight Valley Tillite|44317|4|Described|Table 3, p.7||Adelaidean|||||||
25260|Moonlight Valley Tillite|44318|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
25260|Moonlight Valley Tillite|44324|14|Not recorded|p.10||Adelaidean|Tb.2 (Adelaidean) of Duerdin Group.||||||
25260|Moonlight Valley Tillite|44325|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
25260|Moonlight Valley Tillite|44363|5|Briefly described|p.6,14,17,21|||(Adelaidean) Duerdin Group.||||||
25260|Moonlight Valley Tillite|44364|14|Not recorded|map legend|||||||||
25260|Moonlight Valley Tillite|44868|5|Briefly described|Map Legend||Phanerozoic|||||||
25260|Moonlight Valley Tillite|45041|6|Mentioned|p45|||Refers Dow - Gemuts (1969). Corr. Areyonga Formation||||||
25260|Moonlight Valley Tillite|45047|2|Defined|p87|Adelaidean|Adelaidean|Described pp36, 40.||||||07-NOV-06
25260|Moonlight Valley Tillite|45112|6|Mentioned|p36|||||||||
25260|Moonlight Valley Tillite|45140|6|Mentioned|p59|||||||Lateral equivalent of Redbank Yard Formation.||
25260|Moonlight Valley Tillite|48927|6|Mentioned|Table 1|||Refers Dow and Gemuts (1969)||||||09-AUG-06
25260|Moonlight Valley Tillite|48931|6|Mentioned|p59|||Correlation. Refers Dow and Gemuts(1969)||||||09-AUG-06
25260|Moonlight Valley Tillite|48938|2|Defined|p68|Adelaidean|Adelaidean|||||||
25260|Moonlight Valley Tillite|48943|3|Fully described|p82|||||||||
25260|Moonlight Valley Tillite|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Wolfe Creek Basin. Of Duerdin Group. Unconformably overlies Spencer Sandstone and Shoal Reach Formation. Diamictite, dolostone.||||||07-NOV-06
25260|Moonlight Valley Tillite|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Duerdin Group. Geological Province: Wolfe Creek Basin. Age: c. 610Ma. Massive, matrix-supported, polymictic pebble to boulder conglomerate, poorly sorted massive sandstone, larger clasts polished and striated.||||||
25260|Moonlight Valley Tillite|60682|4|Described|p17 Table 4, 18|Neoproterozoic|Neoproterozoic|Of Duerdin Group. Unconformably overlies Auvergne Group. Conformably overlain by Jarrad Sandstone Member and Beasly Knob Member. Age: 739 +/- 30Ma. Max. thickness: >130m. Geological Province: Wolfe Creek Basin. Diamictite, dolostone.||||||03-MAY-05
25260|Moonlight Valley Tillite|63458|5|Briefly described|p871-874, p877 Tb.1.  |Cryogenian|Cryogenian|East Kimberley region. Dolostone facies deposited by turbidity currents. Isotopic and elemental composition of carbonate unit given. The 'cap dolomicrite' facies is dealt with in detail. See also p883-884, p886-889, p891-p901.||Unit in Duerdin Group.||Overlies Frank River Sandstone. Correlated with Elatina Formation, Landrigan and Walsh Tillites. Is overlain by Ranford Formation.|Uppermost unit is ca. 9 m thick, thinly bedded, cream-pink dolomicrite, which overlies pebble-bearing mudstone and siltstone.|
25260|Moonlight Valley Tillite|63762|5|Briefly described|p19|||See also Moonlight Valley Formation.||||||07-FEB-11
25260|Moonlight Valley Tillite|64104|6|Mentioned|p63|Neoproterozoic|Neoproterozoic|The author proposes this name be replaced by Moonlight Valley Formation "to distinguish stratigraphic terms from genetic interpretation".||||||
25260|Moonlight Valley Tillite|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic |Of Duerdin Group, Wolfe Creek Basin. Diamictite, dolostone ||||||
25260|Moonlight Valley Tillite|65337|5|Briefly described|p94.|Neoproterozoic|Neoproterozoic|One of youngest known units underlying Antrim Plateau Volcanics. Correlated with Marinoan glacial event (late Cryogenian - early Ediacaran) in Adelaide Rift.||||||
25260|Moonlight Valley Tillite|67151|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Wolfe Basin.||Unit in Duerdin Group.||Unconformably overlies Blackfellow Creek Sandstone. Is overlain by Ranford Formation.|Diamictite; laminated dolostone at top.|
25260|Moonlight Valley Tillite|67484|6|Mentioned|p295 Fig.2|Cryogenian|Cryogenian|More commonly referred to as the Moonlight Valley Formation in the text; see also p294-296.||Of the Duerdin Group.||Overlies Frank River Sandstone. Is overlain by Ranford Formation.||
25260|Moonlight Valley Tillite|68244|6|Mentioned|p671|||East Kimberly area, Kimberley region. [Potentially referring specifically to glaciogenic tillitic units within the Moonlight Valley Formation? Or alternate nomenclature to Moonlight Valley Formation].||||||
25260|Moonlight Valley Tillite|68277|6|Mentioned|p95|Neoproterozoic|Neoproterozoic|The rank is not given in the text.||||||
25260|Moonlight Valley Tillite|68473|6|Mentioned|p531-532|||||Duerdin Group||||
25260|Moonlight Valley Tillite|68733|5|Briefly described|p177 Fig.2, p188, p189 Fig.8|Cryogenian|Cryogenian|Victoria and Wolfe Basin.||Of the Duerdin Group.|||Glacigenic sediments.|05-DEC-17
25260|Moonlight Valley Tillite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Wolfe Creek Basin.||Duerdin Group|Includes unnamed finely laminated mudstone and siltstone member||Massive, matrix-supported, polymictic pebble to boulder conglomerate and poorly sorted massive sandstone; larger clasts in conglomerate are polished and striated locally; includes finely laminated mudstone and siltstone member.|30-AUG-18
25260|Moonlight Valley Tillite|69165|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|See also 100k_xsecgeop_lut.csv. ||Duerdin Group|||Massive, matrix supported, polymictic pebble to boulder conglomerate and poorly sorted massive sandstone; larger clasts in conglomerate are polished and striated locally. Finely laminated mudstone and siltstone.|
25260|Moonlight Valley Tillite|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Ediacaran|Victoria/Wolfe Basins, Centralian A Superbasin. Supersequence 3.||Duerdin Group.||Overlies Blackfellow Creek Sandstone. Is overlain by Ranford Formation.||12-JUL-16
25260|Moonlight Valley Tillite|69441|6|Mentioned|p26:1|||Wolfe Basin.||||Correlated with Olympic and Elatina Formations.||12-JUL-16
25260|Moonlight Valley Tillite|69442|5|Briefly described|p27:1-6|||Wolfe Basin. Over 280m thick. Glacial deposits; recognisable by abundant erratics on the residual weathering surface. Represents a continental ice sheet deposit; forms a local striated pavement. Correlated with Uniya Formation, and Elatina Formation (Adelaide Fold Belt).|?635 Ma.|Duerdin Group.||Unconformably overlies Auvergne Group. Is overlain conformably by Beasly Knob Member and (presumably) Jarrad Sandstone Member. Partial lateral equivalent of Bucket Spring Member (Ranford Formation).|Diamictite, dolostone "cap". Erratics are flattened, subrounded, striated, gouged and chatter-marked cobbles and boulders. The most common dropstones are orthoquartzite, sandstone, meta-siltstone, schist, volcanic rocks, granite and dolostone.|12-JUL-16
25260|Moonlight Valley Tillite|69445|5|Briefly described|p30:4, 10, 17|Neoproterozoic|Neoproterozoic|Woolfe Basin. Minor displacement occurs along the Blackfella Creek Fault.||||Is overlain unconformably by Antrim Plateau Volcanics.||12-JUL-16
25260|Moonlight Valley Tillite|69634|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1.|635-541 Ma (Inferred)|Unit of Duerdin Group.|||Massive, matrix-supported, polymictic pebble to boulder conglomerate and poorly sorted massive sandstone; larger clasts in conglomerate are polished and striated locally; finely laminated mudstone and siltstone|
25260|Moonlight Valley Tillite|69673|5|Briefly described|p190|Neoproterozoic|Neoproterozoic|||Duerdin Group|||Tillite with flattened, subrounded, striated and gouged cobbles and boulders.|
25260|Moonlight Valley Tillite|70154|4|Described|100k_interpgeop_lut.csv|Ediacaran|Cryogenian||541-850 Ma|Duerdin Group|||Massive matrix supported polymictic pebble to boulder conglomerate and poorly sorted massive sandstone; finely laminated mudstone and siltstone.|
25260|Moonlight Valley Tillite|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin. ||Duerdin Group|||Diamictite, dolostone.|
25260|Moonlight Valley Tillite|70655|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin.||Duerdin Group.||Shown as unconformably overlying Blackfellow Creek Sandstone. Is shown as overlain by Ranford Formation, Antrim Plateau Volcanics.|Diamictite; laminated dolostone at top.|21-JAN-22
25260|Moonlight Valley Tillite|71267|4|Described|GEOL_LUT_CSV files|Cryogenian|Cryogenian|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|720-635 Ma (inferred)|Unit of Duerdin Group.|||Finely laminated mudstone and siltstone; massive, matrix-supported, polymictic pebble to boulder conglomerate and poorly sorted massive sandstone; larger clasts in conglomerate are polished and striated locally.|
25260|Moonlight Valley Tillite|73083|6|Mentioned|p48||||||||Includes siltstone.|
25260|Moonlight Valley Tillite|73255|4|Described|p532-535, p537, p539, p541-546, p548-550|Ediacaran|Cryogenian|Correlated with the Elatina Glaciation (Corkeron, 2008). 'Cap carbonate' sandstones comprise the top 8-10m of the unit. Base of the Ediacaran is at the base of the 'cap carbonate', 635 Ma. Trough cross-bedded dolomitic sandstone facies deposited in fluvial paleochannels. Evidence of paleosols includes dessication cracks, mineral weathering trends of dolomite, Rivularites repertus microbial trace fossils. Dolomite likely sourced from glacial erosion of the Bungle Bungle Dolomite. Soil type of  paleosols in the upper parts of the unit interpreted as calcic xerosols. Mean annual precipitation estimated to be 265-325 mm based on paleosols, mean annual range of precipitation of 37-48 mm, cool to frigid temperatures. Contains Palaeopascichnus and Yangtziramulus fossils in upper parts. Common early burial alterations include gleisation. Specific locations in text include p534 Fig.2, p539 Fig.6, p542 Fig.10.|635 Ma|Duerdin Group||Overlies the Frank River Sanddstone, conformably underlies the Ranford Formation and Jarrad Member.|Upper 'cap carbonate' contains abundant dolomitic sandstone. Includes trough cross-bedded, medium to coarse dolomitic sandstone, fine-grained sandstone and siltstone laminae between dolomitic sandstone beds, some sandstones contain dolomitic nodules.|
33440|Moorarie Supersuite|22904|6|Mentioned|p57 fig 1|||||||||16-JUL-08
33440|Moorarie Supersuite|23485|4|Described|p20|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
33440|Moorarie Supersuite|23486|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 1830-1780 Ma. Geological Province: Gascoyne Complex||||||07-NOV-08
33440|Moorarie Supersuite|23487|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 1830-1780 Ma. Geological Province: Gascoyne Basin.||||||07-NOV-08
33440|Moorarie Supersuite|23525|4|Described|p22|Paleoproterozoic|Paleoproterozoic|Age: 1830-1780Ma. Geological Province: Gascoyne Complex.||||||07-NOV-08
33440|Moorarie Supersuite|23527|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Complex||||||07-NOV-08
33440|Moorarie Supersuite|23592|5|Briefly described|p13|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
33440|Moorarie Supersuite|23781|5|Briefly described|p5|Paleoproterozoic|Paleoproterozoic|Age: 1830-1780Ma.||||||07-NOV-08
33440|Moorarie Supersuite|24544|4|Described|p3|Paleoproterozoic|Paleoproterozoic|Age: 1830-1780 Ma. Includes potassic and silicic granites, pegmatites. Intrudes Glenburgh Terrane.||||||07-NOV-08
33440|Moorarie Supersuite|44927|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
33440|Moorarie Supersuite|50216|5|Briefly described|p206|Paleoproterozoic|Paleoproterozoic|Of the Gascoyne Complex. Granite and pegmatite. Age: 1830-1780 Ma. Geological Province: Intrudes the boundary between Yilgarn Craton and Glenburgh Terrane (Gascoyne Complex).||||||07-NOV-08
33440|Moorarie Supersuite|50217|6|Mentioned|p222|||||||||
33440|Moorarie Supersuite|50218|5|Briefly described|p240 Fig.2|Paleoproterozoic|Paleoproterozoic|Of the Gascoyne Complex. Includes the Scrubber Granite and Dumbie Granodiorite. Geological Province: Errabiddy Shear Zone.||||||07-FEB-11
33440|Moorarie Supersuite|50219|5|Briefly described|p260 Fig. 2|Paleoproterozoic|Paleoproterozoic|Includes the Scrubber Granite and Dumbie Granodiorite. Granite and pegmatite. Intruded the Camel Hills Metamorphics.  Age: 1830-1790Ma.  Geological Province: Gascoyne Complex.||||||07-FEB-11
33440|Moorarie Supersuite|50220|5|Briefly described|p281 Fig.1|Statherian|Statherian|Granite. Age: 1830-1780 Ma. See also p292 Tb.2.||||||
33440|Moorarie Supersuite|50222|5|Briefly described|p333 Tb. 2|Paleoproterozoic|Paleoproterozoic|Granites in the Narryer (Yarlarweelor Complex) and Glenburgh terranes.  Ages: 1.82Ga and 1.81-1.79Ga.||||||07-NOV-08
33440|Moorarie Supersuite|50223|5|Briefly described|p356|Paleoproterozoic|Paleoproterozoic|Age: 1830-1780Ma (Occhipinti et al, 2001).||||||07-NOV-08
33440|Moorarie Supersuite|50323|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Gascoyne Complex.  Age ~1830-1780Ma.||||||07-NOV-08
33440|Moorarie Supersuite|61262|5|Briefly described|p458 App.|||Age: 1830-1780Ma. See also p446. ||||||
33440|Moorarie Supersuite|63246|5|Briefly described|p478 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 1830-1780Ma. In the Gascoyne Complex.||||||07-NOV-08
33440|Moorarie Supersuite|63469|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Consists of granodiorite, monzogranite, metamonzogranite, metatonalite, metadiorite and gabbro.||||||07-NOV-08
33440|Moorarie Supersuite|63470|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes Gooche Gneiss. Age: c.1830-1780Ma.  Geological Province: Gascoyne Complex. Comprises granodiorites, monzogranites, tonalite, granodiorite to monzogranite, and augen gneiss.||||||07-NOV-08
33440|Moorarie Supersuite|63471|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: 1830-1780Ma. Geological Province: Gascoyne Complex. Comprises monzogranites, tonalite, diorite, gneissose to schistose granodiorite to monzogranite,  local schist, amphibolite, calc-silicate and quartzite.||||||07-NOV-08
33440|Moorarie Supersuite|63866|5|Briefly described|p152, p155, p157, p161, p177|||Ashburton Basin and Glenburgh Terrane.|||Includes the Dumbie Granodiorite and the Scrubber Granite.|Intrudes the Yarlarweelor Gneiss Complex.|I-type granites and pegmatites.|
33440|Moorarie Supersuite|63869|4|Described|p1, p5, p10, p11-13, p16, p25, p46, p47|Paleoproterozoic|Paleoproterozoic|See also p52, Plate 1. Occhipinti and Myers (1999). Developed across the entire width of Gascoyne Complex. Associated with Capricorn Orogeny.|1830-1780 Ma.||Includes Gooche Gneiss.|Intrudes Gascoyne Complex.|Granites and monzogranites, foliated and gneissic granite, granodiorite and tonalite. Includes rafts of quartz-mica schist and metamorphosed fine-grained sandstone.|
33440|Moorarie Supersuite|64161|6|Mentioned|p590|||Gascoyne Complex||||||
33440|Moorarie Supersuite|64580|4|Described|map legend||Paleoproterozoic|Granite and minor gabbro; Metamorphosed foliated and gneissic granite. Two descriptions give age as Paleoproterozoic, one says Devonian.||||||15-DEC-08
33440|Moorarie Supersuite|64722|6|Mentioned|Fig. 2 p3-6|Statherian|Orosirian|Capricorn Orogen?||||||
33440|Moorarie Supersuite|64728|6|Mentioned|p97, pp106-107, p109 Fig.11.|||Metamorphosed granites intruding the Boora Boora Zone of the Gascoyne Complex. A likely source of c.1800 Ma detrital zircons in Bangemall Supergroup.|1830-1780 Ma.||||Granites.|
33440|Moorarie Supersuite|65152|5|Briefly described|p1.|Paleoproterozoic|Paleoproterozoic|Includes Minnie Creek batholith. Intrudes Morrissey Metamorphics.||||||01-MAY-15
33440|Moorarie Supersuite|65450|6|Mentioned|p2 Fig.1, p5 Fig.2, p6 Fig.4|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.||||||
33440|Moorarie Supersuite|65453|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Under Mount Augustus Sandstone and Yilgatherra Formation; intrudes Leake Spring Metamorphics; intruded by Durlacher Supersuite. Age: 1815-1770 Ma. Geol. Prov: Gascoyne Province.||||||
33440|Moorarie Supersuite|65545|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|c. 1815 - 1770 Ma. Consists of various unnamed granites, minor gabbro and metamorphic equivalents.||||||
33440|Moorarie Supersuite|65549|5|Briefly described|Map Legend|Statherian|Orosirian|Of Gascoyne Province. Subdivided into two unnamed units. Age of 1815 - 1770 Ma given.||||||
33440|Moorarie Supersuite|65692|5|Briefly described|p28|Statherian|Orosirian|Gascoyne Complex. Lack of detrital zircons aged 1950-1780 Ma in the basal Earaheedy Basin indicate that this unit was not a sediment source.|1830-1780 Ma.|||||
33440|Moorarie Supersuite|65830|3|Fully described|p25, p26 Fig.13, p27-28, p31, p34, p37|Statherian|Orosirian|See also p39; Plates 1,2. Granites at the northern end of Gascoyne Complex are associated with tungsten-skarn mineralisation.|1830-1780 Ma|Of the Gascoyne Complex.||Intrudes the Morrissey Metamorphics. Emplaced across the Yarlarweelor Gneiss Complex. Overlain by the Pooranoo Metamorphics. Emplaced across the width of the Gascoyne Complex.|Comprises monzogranite and granodiorite, with subordinate to minor syenogranite, tonalite, and quartz diorite; local gabbro intrusions and mafic inclusions.|
33440|Moorarie Supersuite|65896|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Complex. 1830 - 1780 Ma. Includes Kerba Granite.||||||
33440|Moorarie Supersuite|66104|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Age shown as 1817 - 1776 Ma. Massive, medium-grained, porphyritic biotite monzogranite; round phenocrysts of K-feldspar up to 5 cm in diameter; minor fine- to medium-grained, sparsely porphyritic biotite monzogranite.||||||
33440|Moorarie Supersuite|66105|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. 1817-1776 Ma. Includes Rubberoid and Middle Spring Granites, as well as mapped but unnamed units of porphyritic biotite monzogranite, foliated metagranodiorite, and biotite metagranodiorite to metamonzogranite.||||||
33440|Moorarie Supersuite|66110|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Age shown as 1817-1776 Ma. Includes Rubberoid, Middle Spring and Scrubber Granites and Dumbie Granodiorite, and several mapped but unnamed units of monzogranite, metamonzogranite, metagranodiorite, gneisses, metagabbro and schist.||||||
33440|Moorarie Supersuite|66112|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Aged c.1800 Ma. Undivided; granite and minor gabbro and metamorphosed equivalents (interpreted bedrock geology only).||||||
33440|Moorarie Supersuite|66241|4|Described|pp1-4, p6, p29.|Statherian|Orosirian|Gascoyne Province. A relatively fresh granodiorite drillhole sample gave a SHRIMP U-Pb zircon crystallization age of 1797 +/- 8 Ma (Nelson 1995b).|1830 - 1780 Ma (Martin et al. 2005).|||Is unconformably overlain by Kiangi Creek Formation.|Weakly to strongly foliated, porphyritic, coarse-grained granodiorite; locally abundant K-feldspar phenocrysts to 4 cm; includes rafts of strongly foliated psammite and pelite; locally crosscut by thin fluorite veins.|03-MAY-12
33440|Moorarie Supersuite|66299|4|Described|p144-199, p4 Fig.2, p19-22.|Paleoproterozoic|Paleoproterozoic|Includes Minnie Creek batholith which contains small gabbro inclusions. Hosts molybdenum (copper, tungsten) mineralisation. Scarcity of xenocrystic zircons prevents identification of possible sources. About 50 granites from the Supersuite have been dated by SHRIMP U/Pb zircon techniques.|1817 +/- 11 Ma to 1776 +/- 8 Ma. U/Pb SHRIMP||Includes Dumbie Granodiorite, Scrubber, Kerba, Middle Spring and Rubberoid Granites, Gooche Gneiss.|Intrudes Leake Spring, Moogie, Camel Hills Metamorphics, Yarlarweelor Gneiss Complex, Halfway Gneiss, Bertibubba Supersuite. Unconformably overlain by Pooranoo Metamorphics and Edmund Group.|Mostly weakly peraluminous, biotite-bearing monzogranite and granodiorite, with lesser syenogranite, tonalite, quartz diorite.|19-NOV-13
33440|Moorarie Supersuite|66427|5|Briefly described|p41 Tb.1, p49 |||Age in Tb.1 is given as 1.82 Ga for intrusions in Narryer Terrane, and 1.81-1.79 Ga in Glenburgh Terrane.|1780 Ma (Occhipinti et al., 1998).|||||
33440|Moorarie Supersuite|66579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|||Includes Dumbie Granodiorite and Scrubber Granite, as well as two mapped but unnamed units, dominantly monzogranites.||Monzogranites, syenogranites, granodiorites, pegmatites; minor tonalite.|
33440|Moorarie Supersuite|66887|5|Briefly described|p3 Fig.2, p5 Fig.4, p7|Paleoproterozoic|Paleoproterozoic|Southern Gascoyne Province.|1820-1775 Ma|||Stocks and sheets of granite intrude mesocratic unit Halfway Gneiss.|Granite.|
33440|Moorarie Supersuite|66950|5|Briefly described|p3 Fig.2, pp9-15, pp19-27|Orosirian|Orosirian|Gascoyne Province. Mis-spelt as the Moorare Supersuite on p11. The vast majority of granites are magnesian, calc-alkalic, and (weakly) peraluminous.|c. 1820-1800 Ma||Includes the Gooche Gneiss.|Intrudes the Leake Spring Metamorphics and the Asburton Formation of the upper Wyloo Group.|Dominated by granodiorite, monzogranite, and their metamorphosed equivalents.|16-DEC-16
33440|Moorarie Supersuite|67245|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Gascoyne province.||Unit in Bangemall Supersuite.||Is overlain by Yilgatherra Formation.|Massive, equigranular to sparsely porphyritic, biotite monzogranite; medium- and coarse-grained; minor muscovite in places; includes some granodiorite and minor leucocratic tonalite.|
33440|Moorarie Supersuite|67246|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|1811 - 1787 Ma.|||Intrudes Padbury Group. Is overlain nonconformably by Yilgatherra Formation.|Equigranular to sparsely porphyritic biotite tonalite and granodiorite; medium-grained; massive to weakly foliated.|
33440|Moorarie Supersuite|67247|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|1817 - 1776 Ma.||Includes Dumbie Granodiorite and Scrubber Granite.||Undivided: granite and minor gabbro, and metamorphosed equivalents.|
33440|Moorarie Supersuite|67346|6|Mentioned|p794 Fig.1, p795 Fig.2, p796 Fig.3|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|||||Granite.|11-MAY-12
33440|Moorarie Supersuite|67371|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. In this map area, this Supersuite is mapped as 8 separate units, 6 of them un-named.|1811 - 1799 Ma.||Includes Scrubber Granite and Dumbie Granodiorite.||Monzogranites; syenogranites; pegmatites; granodiorites; altered granite.|
33440|Moorarie Supersuite|67373|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|||Includes Dumbie Granodiorite.||Granodiorite, monzogranite, muscovite  monzogranite, pegmatite-banded gneissic and foliated granite.|
33440|Moorarie Supersuite|67843|5|Briefly described|p2 Fig.1, p4, p5, p39.|Paleoproterozoic|Paleoproterozoic|Intruded the Narryer Terrane during the 1820-1770 Ma Capricorn Orogeny to form the Yarlarweelor Gneiss Complex.||||||
33440|Moorarie Supersuite|67888|6|Mentioned|p53|||||||||
33440|Moorarie Supersuite|68055|6|Mentioned|p87|||Gascoyne Province. Associated with the Capricorn Orogeny. Derived fron reworking of continental crust.|||||Voluminous granitic magmas.|
33440|Moorarie Supersuite|68521|5|Briefly described|Map Legend|Statherian|Orosirian|12 sub-units, of which 3 are named, are mapped separately. Geochronology by Evans et al. (2003).|c.1830-1780 Ma||Includes Scrubber Granite, Dumbie Granodiorite, and Rubberoid Granite.|||
33440|Moorarie Supersuite|68522|5|Briefly described|Map Legend|Statherian|Orosirian|Gascoyne Province. 12 sub-units, 3 of which are named, are mapped separately.|1820-1775 Ma||Includes Scrubber Granite, Dumbie Granodiorite, and Rubberoid Granite.|||
33440|Moorarie Supersuite|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv|Paleoproterozoic|Paleoproterozoic|500K_GEOLOGYP08_LUT.csv|||||granite and minor gabbro|
33440|Moorarie Supersuite|68981|5|Briefly described|p19-20|||Gascoyne Province, western Capricorn Orogen.|1820-1775 Ma.||||Voluminous granitic magmas.|
33440|Moorarie Supersuite|69003|5|Briefly described|p4, p9 Fig.9, p26, p33|||Capricorn Orogen. Widespread and extensive granite magmatism associated with the Capricorn Orogeny. Formed by reworking of older crust, not from juvenile mantle-derived material.||||||
33440|Moorarie Supersuite|69011|5|Briefly described|Map Legend|Calymmian|Orosirian|Gascoyne Province. Mapped as 5 unnamed sub-units.|1820-1775 Ma||||Foliated metagranodiorite; medium-grained biotite(-muscovite) granodiorite; leucocratic biotite monzogranite; K-feldspar-porphyritic biotite monzogranite; tonalite with abundant mafic clots and lesser granodiorite with scattered mafic clots.|24-APR-14
33440|Moorarie Supersuite|69028|5|Briefly described|Map Legend|Statherian|Statherian|Gascoyne Province. Also includes an unnamed subunit.|1820-1775 Ma.||Includes the Gooche Gneiss.||Undivided: granite and minor gabbro and metamorphosed equivalents; also strongly foliated, porphyritic metagranodiorite and metamonzogranite, and augen gneiss; massive, subophitic metagabbro, medium grained, amphibolite and minor hornblende schist.|15-AUG-18
33440|Moorarie Supersuite|69080|5|Briefly described|p684, p689, p694 Fig.9, p696-697, p699|Statherian|Orosirian|Gascoyne Province. Intrusion accompanied the Capricorn Orogeny; includes Minnie Creek and Landor batholiths. Constitutes the main suture zone, along the Cardilya Fault, linking the Yilgarn Craton to the composite Pilbara-Bandee-Glenburgh craton, thereby assembling the West Australian Craton.|1820-1775 Ma.||||Granite and minor gabbro and metamorphosed equivalents.|
33440|Moorarie Supersuite|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Age derived from samples of granite and metatonalite (185951.1.pdf, 190685.1.pdf)|1784 +/- 3Ma, 1811 +/- 5 Ma  (SHRIMP)||Includes Dumbie Granodiorite, Gooche Gneiss, Middle Spring Granite, Rubberoid Granite, Scrubber Granite|Intrudes Yarlarweelor Gneiss Complex|Granite, gabbro,  biotite-muscovite granodiorite, biotite muscovite granodiorite or monzogranites. Metamonzogranite, leucocratic porphyritic micromonzogranite,  syenogranite, pegmatite, metagranodiorite, metatonalite, metagranite, metagabbro.|
33440|Moorarie Supersuite|69185|4|Described|500k_geologyp08_lut.csv||Paleoproterozoic|Geological Province: Pilbara Craton.|||Includes Gooche Gneiss.||Metamorphosed foliated and gneissic granite|
33440|Moorarie Supersuite|69237|6|Mentioned|p2|Statherian|Orosirian|Gascoyne Province.||||||
33440|Moorarie Supersuite|69387|4|Described|p3, p7, p9, p11-35, p37, p52, p68|Statherian|Orosirian|Gascoyne Province. Associated with the Capricorn Orogeny. Very common and widespread. Includes the Minnie Creek batholith. Deformations discussed; structural fabric diagrams. SG and magnetic susceptibility values given. Gravity and magnetic modelling. Consists largely of large batholiths, ~5 to 10km thick, with tabular geometries. Hosts uraniferous and base metal quartz vein mineralisation with Cu-Pb sulfides at Mundong Well; also W-skarn mineralisation in the N of the Province.|1820-1775 Ma.||Erong Granite.|Is intruded by Durlacher Supersuite.|Voluminous, felsic magmatic stocks and plutons: tonalites, quartz diorites and some metagabbro. I-type (Na-rich). Oxidised and fractionated.|
33440|Moorarie Supersuite|69546|5|Briefly described|p102|Statherian|Orosirian|Geological province: Gascoyne Province.|1830-1780 Ma|||||
33440|Moorarie Supersuite|69583|5|Briefly described|p130, Plate 3.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|1817-1773 Ma.||||Undivided: granite and minor gabbro, and metamorphosed equivalents.|
33440|Moorarie Supersuite|69596|5|Briefly described|p4-6, p9|Paleoproterozoic|Paleoproterozoic|Capricorn Orogen.|1820-1775 Ma.|||Is overlain unconformably by Edmund Group.||
33440|Moorarie Supersuite|70019|5|Briefly described|p92,94|Orosirian|Orosirian|Geological province: Gascoyne Province, Capricorn Orogen. Comprises Neoarchean to Paleoproterozoic basement rock assemblage of the Gascoyne Province. Emplaced during Capricorn Orogeny.|1820-1775 Ma|||||
33440|Moorarie Supersuite|70127|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. The three un-named facies are mapped separately.|1817-1773 Ma.||||Pale grey, foliated and gneissic metamonzogranite; foliated and gneissic metagranodiorite and metatonalite, weakly pegmatite banded; fine- to medium-grained, foliated metagranodiorite, locally porphyritic.|
33440|Moorarie Supersuite|70132|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|1795-1792 Ma.||||Massive, medium-grained, porphyritic biotite monzogranite; round phenocrysts of K-feldspar up to 5cm diameter; minor fine- to medium-grained, sparsely porphyritic biotite monzogranite.|
33440|Moorarie Supersuite|70138|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|1817-1773 Ma.|||Is overlain by Nannyarra Sandstone.|Metagabbro, amphibolite, tonalite, monzogranite, granodiorite, biotite(-muscovite) granodiorite, foliated and gneissic metagranodiorite and metatonalite.|
33440|Moorarie Supersuite|70767|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Section only: no outcrop in map area.|1817-1773 Ma.||||Granite and minor gabbro, and metamorphosed equivalents.|
33440|Moorarie Supersuite|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 2_5m_interpgeop15_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 88407.1.pdf, 169810.1.pdf, West Australian Craton, intrudes into Gascoyne province, Yarlarweelor Gneiss Complex and Ashburton Basin|1830-1773 Ma|||Unconformably overlain by Kiangi Creek Formation, Intrudes Labouchere Formation, Moogie Metamorphics and Leake Spring Metamorphics, Halfway Gneiss and Dalgaringa Supersuite|Metagranodiorite, metamonzogranite, metatonalite, leucocratic metamonzogranite, metagranite, pegmatite, leucocratic granitic gneiss, schistose and gneissic metamonzogranites, metatonalite, metadiorite, metagabbro, granodiorite and micromonzogranite.|
33440|Moorarie Supersuite|70796|4|Described|2_5m_interpgeop15_lut.csv|Paleoproterozoic|Paleoproterozoic|Of the Capricorn Orogen, Gascoyne Province. Affected by the following events:  Mulka Tectonic Event (570  570 Ma); Edmundian Orogeny D3e/M3e (995  954 Ma); Edmundian Orogeny (1026  954 Ma); Edmundian Orogeny D1e/M1e (1026  995 Ma); Edmundian Orogeny D2e/M2e (1026  995 Ma); Mutherbukin Tectonic Event (1321  1171 Ma); Mangaroon. A minimum age of 1773 is infered. See also 500k_interpgeop14_lut.csv.|1817 +/ 11 Ma (Max age, isotopic)||||Granite and minor gabbro, and metamorphosed equivalents|
33440|Moorarie Supersuite|70814|5|Briefly described|p4, p8-p9, p27, p62|Statherian|Orosirian||1820-1775 Ma|||Disconformably overlain by the Irregully and Kiangi Creek Formations.||
33440|Moorarie Supersuite|70826|6|Mentioned|p9, p10|Paleoproterozoic|Paleoproterozoic|Intruded during the Capricorn Orogeny.|1817-1772 Ma (Capricorn Orogeny)|||Intrudes the Yarlarweelor Gneiss Complex.|Granitic gneisses.|
33440|Moorarie Supersuite|71000|6|Mentioned|p65|Paleoproterozoic|Paleoproterozoic|Southern Gascoyne Province.||||||
33440|Moorarie Supersuite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, granodiorite, tonalite|
33440|Moorarie Supersuite|71269|5|Briefly described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Gascoyne Province; Capricorn Orogen, West Australian Craton. Events: Mulka Tectonic Event (570-570 Ma); Edmundian Orogeny D3e/M3e (995-954 Ma); Edmundian Orogeny (1026-954 Ma); Edmundian Orogeny D1e/M1e (1026-995 Ma); Edmundian Orogeny D2e/M2e (1026-995 Ma); Mutherbukin Tectonic Event (1321-1171 Ma); Mangaroon??. See 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|1817+\-11 Ma; 1773 Ma (isotopic; inferred)||||Granite and minor gabbro, and metamorphosed equivalents|
33440|Moorarie Supersuite|71273|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|1817-1773 Ma.||Boolaloo Granodiorite.||Foliated and gneissic metagranodiorite, metatonalite and metamonzogranite.|
33440|Moorarie Supersuite|71484|5|Briefly described|p125|||Geological province: Of Padbury Basin [?].||Unit of Padbury Group.|Includes Kerba Granite.|Underlain by Millidie Creek Formation.|Granite, micro gabbro, metamorphosed equivalents.|30-AUG-19
33440|Moorarie Supersuite|71804|6|Mentioned|p403 fig 10|||Gascoyne Province.||||||
33440|Moorarie Supersuite|71869|5|Briefly described|p2-p4, p6, p9, p11-p13, p15-p18, app p5,|||Capricorn Orogen.|c. 1820-1770 Ma||Includes the Dumbie Granodiorite, Scrubber Granite, Rubberoid Granite, Middle Spring Granite, Booaloo Granodiorite and Gooche Gneiss.||Granodiorite dykes, monzogranite, granites, metatonalite.|
33440|Moorarie Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Gascoyne Province, Capricorn Orogen. Supersuite and one unnamed sub-unit listed.|Max age 1817+/-11 Ma, min ~1773 Ma.||||Granite and minor gabbro, and metamorphosed equivalents. Massive, subophitic metagabbro; medium grained; amphibolite; minor hornblende schist.|
33440|Moorarie Supersuite|72259|6|Mentioned|p3, App. Tb.B|Statherian|Orosirian||ca. 1820-1775 Ma||||Includes quartz-muscovite mylonite and biotite-muscovite granodiorite.|
33440|Moorarie Supersuite|72705|6|Mentioned|p3, 14|||Capricorn Orogen. Voluminous felsic magmatism associated with the Capricorn Orogeny.|1820 - 1775 Ma.|||||
33440|Moorarie Supersuite|73102|5|Briefly described|p3, p8|Statherian|Orosirian|Gascoyne Province.|1817-1773 Ma|||Intruded by Minga Dolerite.|Granite and minor gabbro and metamorphosed equivalent.|
33440|Moorarie Supersuite|73168|6|Mentioned|p758, 765|||Gascoyne Province. Glenburgh Terrane. Emplaced during the intraplate Capricorn Orogeny.||||||
33440|Moorarie Supersuite|73214|5|Briefly described|p974 Fig.1, 975, 985-986, 988|Palaeoproterozoic|Palaeoproterozoic|Northern Gascoyne Province. Affected by the 1820-1775 Ma Capricorn Orogeny. Max and min ages are based on the oldest intrusion and youngest metamorphic zircon rim, respectively.|1820-1775 Ma.||||Voluminous felsic magmatic stocks, plutons and batholiths.|
33440|Moorarie Supersuite|73442|5|Briefly described|p3|||Gascoyne Province.|||||Granite and minor gabbro and metamorphosed equivalents.|
36989|Moore Porphyry|23470|5|Briefly described|p125|Archean|Archean|Age: 2669 +/-7 Ma. Geological Province: Yilgarn Craton.||||||07-NOV-08
39514|Mopoke Member|63367|5|Briefly described|p230, p234 Tb.1.  |Neoarchean|Neoarchean|Trace elements and REE + Y data discussed in detail.||Of the Kylena Formation (Fortescue Group).|||Silicified blue-grey limestone/dolomite with thin blue chert beds; capped by ripple marked siltstone; stromatolites.|
39514|Mopoke Member|65724|5|Briefly described|map legend|Neoarchean|Neoarchean|Of Kylena Formation. Grey carbonate rock; discontinuous, silicified microbial laminations and stromatolite; minor shale, siltstone and sandstone. Geol. Prov: Hamersley Basin, Pilbara Craton.||||||05-DEC-11
39514|Mopoke Member|65726|5|Briefly described|Map legend|Archean|Archean|Hamersley Basin, Pilbara Craton.||Of Kylena Formation.|||Grey carbonate rock; discontinuous, silicified microbial laminations and stromatolites; minor shale and siltstone.|
39514|Mopoke Member|65727|5|Briefly described|Map legend|Neoarchean|Neoarchean|Fortescue Basin.||Of Kylena Formation.|||Grey carbonate rock; discontinuous, silicified microbial laminations and stromatolites; minor shale, siltstone and sandstone.|
39514|Mopoke Member|65827|3|Fully described|p12 Tb.3, p33 Fig.6, p37, p40|Neoarchean|Neoarchean|Of Kylena Formation (Fortescue Group). 2749-2735 Ma. Thin lacustrine stromatolitic carbonate underlain, overlain and interbedded with calcareous siltstone, shale, mudstone; shown as equivalent to part of Nullagine Supersequence. Separates two compositionally different basalt successions in the Kylena Formation.||||||
39514|Mopoke Member|65829|2|Defined|p10, pp18-19, p22,  pp43-44.|Neoarchean|Neoarchean|New name. Named after Mopoke Well. Exposed discontinuously across the southwest quarter of the map area. Type areas include prominent low cliff-lines on southern side of Ripon Hills road, 7.5 km northwest of Bookabunna Well. It is a useful marker bed in the lower third of the Kylena Formation. Represents a pause in volcanic activity. Intruded by thick dolerite sills and dykes.|Between c.2735 Ma and c.2727 Ma.|Unit in Kylena Formation.||Overlies unconformably the Midgengadgi Monzogranite and Little River Trondhjemite.|Silicified blue-grey limestone or dolomitic limestone to 5 m thick; interbedded and overlain by thin-bedded, calcareous and tuffaceous siltstone and shale, fine sandstone and thin blue chert beds. Thin lacustrine stromatolitic carbonates.|
39514|Mopoke Member|68101|4|Described|p1-10|Neoarchean|Neoarchean|Williams (2007). 0-15m thick grey, cliff-forming marker horizon, separating two compositionally distinct basalt successions. Oldest fossiliferous carbonate unit in the Fortescue Group. Lithology and stromatolites are described in detail. Ripple marks are distinctive. Age range from surrounding units.|Between 2736 +/- 6 Ma and 2721 Ma.|Kylena Formation|||Cherty stromatolitic carbonate, wavy laminated and recrystallized stromatolitic carbonate, fine sandstone, tuffaceous or calcareous mudstone, cherty carbonate breccia, edgewise conglomerates, kerogenous siltstone and shale, basaltic agglomerate.|
39514|Mopoke Member|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Kylena Formation|||Grey carbonate rock; discontinuous, silicified microbial laminations and stromatolites; minor shale, siltstone, and sandstone.|
39514|Mopoke Member|69411|5|Briefly described|p293|Neoarchean|Neoarchean|Geological province: Pilbara Craton. ||Unit of Kylena Formation.||||
39514|Mopoke Member|69590|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Of Northeast Pilbara Sub-basin, Fortescue Basin. Events: Pilbara Craton breakup. See 100k_geologyp_lut.csv, 100k_geologyl_lut.csv.|2749-2735 Ma (isotopic, inferred)|Unit of Kylena Formation.|||Grey carbonate rock; discontinuous, silicified microbial laminations and stromatolites; minor shale, siltstone, and sandstone|
39514|Mopoke Member|69792|5|Briefly described|p1095-1107|Neoarchean|Neoarchean|A laterally extensive stromatolitic carbonate horizon. Four lithofacies discussed in detail. Contains the oldest stromatolitic horizon in Fortescue Group. Probably an upwards-shallowing, shallow marine depositional environment: features mud-draped (tidal) ripples and overlies pillow basalts. 13C (carbonate and organic) and 18O isotope data detailed.|c.2.74 Ga.|Unit in Kylena Formation.|||Siltstone/mudstone with calcilutite in cm-thick beds; local basal stromatolitic carbonate, intraformational conglomerate or lithic sandstone. Spar, dolospar and radiaxial calcite are conspicuous.|
68140|Morangup Hill laterites|60901|6|Mentioned|p907|Late Miocene|Late Miocene|Not intended as a formal name.||||||
35678|Morgan Island Epiclastic|23137|4|Described|p245 Table.2|||of Black Flag Group.||||||
26753|Mornington Volcanics|29549|5|Briefly described|p201|||||||||
26753|Mornington Volcanics|31446|6|Mentioned|p7|||Refers to Guppy et al., (1958). SD51-15,16.||||||
26753|Mornington Volcanics|31828|6|Mentioned|p32|||See also P47. Lateritisation & bauxite.||||||
26753|Mornington Volcanics|32663|6|Mentioned|p10|||||||||
26753|Mornington Volcanics|39796|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
26753|Mornington Volcanics|44998|14|Not recorded|p17|||||||||
26753|Mornington Volcanics|48874|14|Not recorded|Tb.I.p.16|||||||||
80125|Mosquito Well Conglomerate Member|71212|5|Briefly described|intro p2|||Yilgarn Craton. ||Vivien Formation|||Conglomerates.|
80125|Mosquito Well Conglomerate Member|73151|5|Briefly described|p2-3, p5, p7, p13, p15|Neoarchean|Neoarchean|Yilgarn Craton, Kalgoorlie Terrane. Up to 100 m thick with wedge-shaped distribution in the Vivien Formation, consistent with emplacement on slope apron by mass flows.||Vivien Formation||Unconformably overlies Kalgoorlie Group.|Polymictic conglomerate dominated by aphyric to porphyritic mafic and felsic volcanic clasts. Conglomerate is massive, poorly sorted, clast-supported and contains a sandy matrix, clasts are sub-rounded to well-rounded.|
80125|Mosquito Well Conglomerate Member|73596|6|Mentioned|p1157|Neoarchean|Neoarchean|"Agnew-Wiluna Greenstone Belt. Only locally developed. The ""conglomerate"" part of the name occurs further along in the sentence."||Basal Vivien Formation.|||Conglomerate. Contains clasts of dolerite (similar to Turret Dolerite).|
34556|Mosswood Formation|12758|4|Described|p11, p3 Fig. 3|Early Permian|Early Permian|Classified with the expanded Stockton Group (Collie Basin) by LeBlanc-Smith and Kristensen (1998), maintained in this study.  Overlain conformably by the Sue Group.  Geological Province: Southern Perth Basin.See also p57.||||||19-OCT-04
34556|Mosswood Formation|14227|5|Briefly described|p9, Enclos. 2|Early Permian|Carboniferous|Underlies the Sue Group. Glacial sediments. Geol. Prov: Bunbury Trough, Perth Basin.||||||07-FEB-11
34556|Mosswood Formation|22818|5|Briefly described|map|Early Permian|Early Permian|Stockton Group||||||
34556|Mosswood Formation|22819|5|Briefly described|map|Late Permian|Early Permian|Stockton Group||||||
34556|Mosswood Formation|22820|2|Defined|p8 Tb. 1, p13-14|Early Permian|Early Permian|Of Stockton Group. Grades up into Woodynook Sandstone. Geol. prov: southern Perth Basin. Pro-deltaic, siliciclastic rocks: upward-coarsening sequence of dark grey shale and siltstone. Detailed lithology included.||||||12-AUG-08
34556|Mosswood Formation|24443|5|Briefly described|Fig.31|Early Permian|Early Permian|Overlies Precambrian basement. Overlain conformably by Woodynook Sandstone of Sue Group. Geological Province: Perth Basin.||||||
34556|Mosswood Formation|50107|5|Briefly described|Map legend|Permian|Permian|Geological Province: Southern Perth Basin.||||||
34556|Mosswood Formation|60386|6|Mentioned|p296|Sakmarian|Asselian|Perth Basin. Non-marine.||||||
34556|Mosswood Formation|64630|5|Briefly described|p31 Fig.2|Sakmarian|Asselian|Province: Southern Perth Basin. Overlies the Cullens Diamictite, underlies the Woodynook Sandstone. Palynology age: P. confluens. Correlates with the Moorehead Formation.||||||12-SEP-13
34556|Mosswood Formation|64981|6|Mentioned|p670.|||Perth Basin. Regional transgression at the base of this unit and Mosswood Formation in Perth Basin, and Lyons Group in Carnarvon Basin, may be coeval with partial melting of extensive Carboniferous ice caps.||||||
34556|Mosswood Formation|67925|4|Described|Ch2 p10 fig 4, Ch2 p13, Ch2 p20|Sakmarian|Asselian |Unconformably overlies the basement of the Southern Perth basin. Interpreted to have been deposited in a fluvio-lacustrine environment. In the Sue 1 drillhole is up to 1060m thick. Palynology discussed. See also Ch2 p26-p27, Ch2 p30, Ch3 p8, Ch3 p15 , Ch4 p8 fig 2.|||Includes the Cullens Diamictite.|Overlain by the Sue Group and the Woodynook Sandstone.|Dark grey-brown to black argillaceous rocks with subordinate siltstone and fine-grained sandstone.|
34556|Mosswood Formation|69029|6|Mentioned|p332|Cisuralian|Cisuralian|Of Perth Basin.||||Overlain by Holmwood Shale. Underlain by Nangetty Formation.||
34556|Mosswood Formation|69081|6|Mentioned|p737 Fig.1|Cisuralian|Cisuralian|Geol. Prov: Perth Basin||||||
34556|Mosswood Formation|69182|6|Mentioned|Ch2 p9, Ch2 p11|Early Permian|Early Permian|Perth Basin. See also Ch2 p45, Ch2 p47-p49  Ch2 p55, Ch2 p57, Ch2 p60, Ch2 p64-p66, Ch2 p80, Ch2 p84, Ch2 p92, Ch2 p94-p96, Ch2 p98, Ch2 p100, Ch2 p102, Ch2 p104, Ch2 p106, Ch2 p108, Ch2 p110.||Stockton Group||Overlies the Cullens Diamictite. Overlain by the Woodynook Sandstone.||
34556|Mosswood Formation|69297|6|Mentioned|p175, p187, p189|Sakmarian|Asselian|Vlaming Sub-basin, South Perth Basin. ||Stockton Group||Overlain by the Woodynook Sandstone.||
34556|Mosswood Formation|70097|5|Briefly described|p2, p19 Fig.3|Sakmarian|Asselian|Southern Perth Basin. Bunbury Trough.||Stockton Group.|Cullens Diamictite|Is overlain by Woodynook Sandstone (Sue Group).|Glacial basin fill. Shale.|12-SEP-17
34556|Mosswood Formation|70099|5|Briefly described|Fig.4|Sakmarian|Asselian|||Stockton Group.||Is overlain by Woodynook Sandstone (Sue Group).||
34556|Mosswood Formation|70128|5|Briefly described|p449|Permian|Permian|Southern Perth Basin.||||Is overlain conformably by Woodynook Sandstone (Sue Group).||
34556|Mosswood Formation|70774|5|Briefly described|p5 fig 3|Sakmarian|Sakmarian|Southern Perth Basin.||||Overlies the Cullens Diamictite. Overlain by the Woodynook Sandstone.||
34556|Mosswood Formation|71146|5|Briefly described|p6|Sakmarian|Sakmarian|Perth Basin.||||Overlies the Cullens Diamictite. Overlain by the Woodynook Sandstone.|Mudstone.|
34556|Mosswood Formation|71377|5|Briefly described|p7|Permian|Carboniferous|Perth Basin.||Stockton Group||||
34556|Mosswood Formation|71958|5|Briefly described|p34|Sakmarian|Asselian|Vlaming Sub-basin.||||Overlain by the Woodynook Sandstone (Sue Group).||
34556|Mosswood Formation|72258|5|Briefly described|p129|Cisuralian|Cisuralian|Of Perth Basin.||||Overlain by Woodynook Sandstone. Underlain by crystalline basement.||
34556|Mosswood Formation|73117|6|Mentioned|p35|||Perth Basin, southern. Glacigene. Lateral equivalent of the Stockton Formation in both age and facies.||||Equivalent to Stockton Formation.||
38073|Motherin Monzogranite|24166|4|Described|p17|Archean|Archean|Dated at c. 3475 Ma. Of the Carlindi Granitoid Complex.||||||15-APR-13
38073|Motherin Monzogranite|24327|5|Briefly described|Map Legend|Archean|Archean|Of the Carlindi Granitoid Complex. Interleaved monzogranite, granodiorite, gneiss and pegmatite. Age: c. 3475 Ma. Geological Province: Pilbara Craton.||||||15-APR-13
38073|Motherin Monzogranite|24349|5|Briefly described|Map legend|Archean|Archean|Of the Carlindi Granitoid Complex. Age: c. 3475 Ma. Geological Province: Pilbara Craton||||||15-APR-13
38073|Motherin Monzogranite|50379|5|Briefly described|Map Legend|Archean|Archean|Of the Carlindi Granitoid Complex. Age: c. 3475 Ma. Geological Province: Pilbara Craton.||||||15-APR-13
38073|Motherin Monzogranite|63420|5|Briefly described|Map legend|Archean|Archean|Of Callina Supersuite. Age: c. 3475 Ma. Geol.Prov: Pilbara Craton. Interleaved metamonzogranite, metagranodiorite, granitic gneiss and pegmatite; moderately to strongly foliated; intruded by abundant sheets of massive to weakly foliated muscovite/pegmatite.||||||15-APR-13
38073|Motherin Monzogranite|63441|5|Briefly described|p7 Tb. 2|Archean|Archean|Of the Callina Supersuite. Age: c. 3475 Ma. Geological province: Pilbara Craton.||||||15-APR-13
38073|Motherin Monzogranite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Callina Supersuite. Interleaved metamonzogranite, metagranodiorite, gneiss, and pegmatite; moderately to strongly foliated; intruded by abundant sheets of massive to weakly foliated muscovite-bearing metamonzogranite and pegmatite.||||||
38073|Motherin Monzogranite|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c. 3475 Ma|Of the Callina Supersuite.|||Interleaved metamonzogranite, metagranodiorite, gneiss, and pegmatite; moderately to strongly foliated; intruded by abundant sheets of massive to weakly foliated muscovite-bearing metamonzogranite and pegmatite.|
38073|Motherin Monzogranite|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Callina Supersuite.|||Interleaved metamonzogranite, metagranodiorite, granitic gneiss, and pegmatite; moderately to strongly foliated; intruded by abundant sheets of massive to weakly foliated muscovite-bearing monzogranite and pegmatite.|06-JAN-15
38073|Motherin Monzogranite|69013|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane. An unnamed biotite and muscovite-biotite monzogranite, massive to weakly foliated, facies of the Mesoarchean Split Rock Supersuite forms pods and larger bodies in the Motherin Monzogranite.|c. 3475 Ma|Of the Callina Supersuite.|||Comprises interleaved metamonzogranite, metagranodiorite, gneiss, and pegmatite; moderately to strongly foliated; intruded by abundant sheets of massive to weakly foliated muscovite-bearing metamonzogranite and pegmatite.|16-NOV-16
38073|Motherin Monzogranite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Age derived from sample of strongly foliated to gneissic syenogranite (169021.2.pdf) and is the age of igneous crystallisation of syenogranite protolith|2923 Ma +/- 3 Ma (SHRIMP)|Callina Supersuite|||Interleaved metamonzogranite, metagranodiorite, gneiss, and pegmatite; moderately to strongly foliated; intruded by abundant sheets of massive to weakly foliated muscovite-bearing metamonzogranite and pegmatite|
38073|Motherin Monzogranite|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA 169021 (gneissic leucocratic syenogranite) yielded an an interpreted igneous crystalllisation age of 2923+\-3 Ma, and metamorphic episodes at 2915+\-3 and 2903+\-3 Ma.  See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|3475-3462 Ma (inferred)|Unit of Callina Supersuite.|||Interleaved metamonzogranite, metagranodiorite, gneiss, and pegmatite; moderately to strongly foliated; intruded by abundant sheets of massive to weakly foliated muscovite-bearing metamonzogranite and pegmatite|
38073|Motherin Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||pegmatite, felsic gneiss, monzogranite, granodiorite, gneiss|
38073|Motherin Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|||Callina Supersuite|||Interleaved metamonzogranite, metagranodiorite, gneiss, and pegmatite; moderately to strongly foliated; intruded by abundant sheets of massive to weakly foliated muscovite-bearing metamonzogranite and pegmatite.|
22395|Mougooderra Formation|22774|6|Mentioned|Fig.2 p573|||||||||
22395|Mougooderra Formation|44149|5|Briefly described|p33 fig 2-29, p35 fig 2-30, p34, p42-46|Archean|Archean|See also p58 Fig.2-72, p59 Fig.2-74. Of Murchison Province. Perhaps up to 3 km thickness of the only substantial epiclastic sedimentary deposit in the Murchison Supergroup. Upward-fining. Conglomerate clasts from Luke Creek Formation.||Mount Farmer Group||Unconformably overlies Luke Creek Group. Sheared contact with ?underlying Singleton Basalt.|Basal immature lithic wacke with abundant conglomerate beds and lenses, then bedded sandstone and shale with preserved sedimentary structures; at top are fine grained shale and siltstone; pyritic black shale in fresh exposure. Local basalt units.|
22395|Mougooderra Formation|61144|6|Mentioned|p13|||||||||
22395|Mougooderra Formation|64891|6|Mentioned|p36|||Rocks include both coarse clastic sediments and komatiitic basalt - authors suggest separate formation status for thes two very different rock types.||||||07-FEB-11
22395|Mougooderra Formation|65268|6|Mentioned|p6 fig 4, p5 fig 3|||||Unit in Mount Farmer Group.|||Epiclastic sedimentary rocks.|
22395|Mougooderra Formation|69267|6|Mentioned|p654|||Murchison Province, Yilgarn Craton.||Mount Farmer Group.||||
22395|Mougooderra Formation|69583|5|Briefly described|p49|Neoarchean|Neoarchean|Murchison Domain.||Polelle Group.||||
22395|Mougooderra Formation|69584|5|Briefly described|p5 Fig.2|Neoarchean|Neoarchean|||Polelle Group||Overlies the Yaloginda Formation, overlain by the Meekatharra Formation|Quartzite and banded-iron formation.|
22395|Mougooderra Formation|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Polelle Group.||||
22395|Mougooderra Formation|70020|5|Briefly described|p118|Neoarchean|Neoarchean|Geological province: Yilgarn Craton.||Unit of Polelle Group.||Overlain by Meekatharra Formation. Underlain by Yalogina Formation/Norie Group.||
22395|Mougooderra Formation|70226|5|Briefly described|Map legend.|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Carton.|<c.2746 Ma.|Glen Group|||Conglomerate, pebbly sandstone, sandstone, quartzite and quartz-rich sandstone, siltstone, mudstone, shale. Also, basalt; schistose pelite/psammite; rhyolitic/dacitic volcanic and volcaniclastic rock; all metamorphosed, commonly deeply weathered.|16-DEC-15
22395|Mougooderra Formation|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton. Six facies are mapped separately.||Glen Group.|||BIF and minor banded chert, granular texture; conglomerate, pebbly sandstone, sandstone; strongly foliated conglomerate; sandstone, siltstone, local conglomerate; quartzite and quartz-rich sandstone; schistose pelite and psammite. All metamorphosed.|
22395|Mougooderra Formation|70796|5|Briefly described|100k_geologyl_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv,  500k_interpgeop_lut.csv, 198295.1.pdf, 211101.1.pdf. Numerous additional lithologies are discussed.|ca 7235 Ma2700 Ma (inferred)|Glen Group||Unconformably overlies the Polelle and Norie groups.|Quartzite and metamorphosed quartzrich sandstone, metasedimentary rock, metamorphosed banded iron formation and minor banded chert. Schistose pelite and psammite; Felsic, rhyolitic and dacitic volcanic and volcaniclastic rocks.|
22395|Mougooderra Formation|71168|4|Described|p7|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c. 2790 Ma|Polelle Group||Overlies the Yaloginda Formation. Overlain by the Meekatharra Formation.|Quartzite and banded-iron formation.|
22395|Mougooderra Formation|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Confined to SE Murchison Domain. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). Lu et al., (2016a) dated a metamorphosed quartz diorite at 2801+\-6 Ma; Lu et al. (2016b) provided maximum depositional age of 2826+\-7 Ma for a sample of volcaniclastic metasandstone. Sample GSWA 198295 (fine-grained metadacite) yielded a weighted mean 207Pb/206Pb date of 2801+\-5 Ma, interpreted as a maximum crystallization age for the dacite (zircons intrepreted as xenocrysts). Sample GSWA 211101 (volcaniclastic mudstone) yielded a weighted mean 207Pb/206Pb date of 2758+\-4 Ma, interpreted as a maximum depositional age for the volcaniclastic mudstone. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeol_lut.csv.|2735-2700 Ma|Unit of Glen Group.||Underlain by Polelle and Norie groups.|Schistose pelite and psammite; includes metamorphosed shale and siltstone; felsic volcanics, volcaniclastics; rhyolitic, dacitic volcanics, volcaniclastics; basalt, pillowed, vesicular; sandstone, siltstone, mudstone, conglomerate; metamorphosed.|
22395|Mougooderra Formation|71272|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. The six facies are mapped separately.||Glen Group.|||Granite with coarse amphibolitic xenoliths; conglomerate, pebbly sandstone and sandstone; sandstone, siltstone, local conglomerate; felsic volcanic, volcaniclastic and sedimentary rocks; quartzite; schistose pelite and psammite. All metamorphosed.|
22395|Mougooderra Formation|71809|5|Briefly described|map legend|Archean|Archean|Yilgarn Craton, Youanmi Terrane|<2746 Ma|Of Glen Group.|||Metasandstone interbedded with polymictic metaconglomerate, metasiltstone and metamorphosed banded iron formation; minor felsic, andesitic and basaltic volcanic units; locally strongly deformed; common andalusite and contact metamorphic aureoles.|
22395|Mougooderra Formation|73023|5|Briefly described|p1-7, 9-16|Neoarchaean|Neoarchaean|Youanmi Terrane, Yilgarn Craton. One of the largest epiclastic metasedimentary sequences within this Terrane. 2 - 3 km thick. P-T metamorphic conditions analysed. Metamorphosed at 2686 +/- 18 Ma: late prograde garnet growth. The article suggests metamorphism is consistent with lithospheric extension and onset of a mantle plume event across the Yilgarn Craton. Geochemistry, petrography, mineralogy tabulated/discussed.|2758 +/- 4 Ma (MDA: zircon, Liu et al., 2016).|||Unconformably overlies Polelle and Norie Groups. Is intruded by Seeligson Monzogranite.|Interbedded conglomerate, sandstone and siltstone, with minor BIF.|
22395|Mougooderra Formation|73410|5|Briefly described|p2|||Youanmi Terrane.|c.2750 Ma.||||Greenstone.|
26045|Mount Ada Basalt|23046|5|Briefly described|169|||||||||
26045|Mount Ada Basalt|23416|5|Briefly described|Map Legend|Archean|Archean|Of Talga Talga Subgroup, Pilbara Craton||||||07-NOV-08
26045|Mount Ada Basalt|23755|4|Described|p19|Archean|Archean|See also page 17 table 1. Age: 3522+/-13 Ma. Of Warrawoona Group.  Max. thickness: 300 m.||||||07-NOV-08
26045|Mount Ada Basalt|23780|5|Briefly described|p149|||Overlain by Duffer Formation.||||||25-JUL-07
26045|Mount Ada Basalt|23783|5|Briefly described|p11|||Of Talga Talga Subgroup.||||||
26045|Mount Ada Basalt|23807|6|Mentioned|p110 Fig. 2|||Mount is Mt in text.  Geological Province: Pilbara Craton.||||||
26045|Mount Ada Basalt|23813|5|Briefly described|p91 Tb. 1|Archean|Archean|Of the Warrawoona Group.  Age: c.3.48-3.43Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.||||||07-NOV-08
26045|Mount Ada Basalt|24025|4|Described|p9 Tb. 1|Archean|Archean|Of Talga Talga Subgroup.  Massive basalt, pillow basalt, and chert.  Max. Thickness: 2500m.  Geological Province: Pilbara Craton.||||||07-NOV-08
26045|Mount Ada Basalt|24184|6|Mentioned|p700|Archean|Archean|Of the Talga Talga Subgroup. Geological Province: Pilbara Craton. Age: ca.3473-3463Ma. Locally interbedded with Duffer Formation.||||||07-NOV-08
26045|Mount Ada Basalt|24185|5|Briefly described|p746 Tb.4|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
26045|Mount Ada Basalt|24194|5|Briefly described|p905|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
26045|Mount Ada Basalt|24590|5|Briefly described|p29, p30 Fig. 1.3|Archean|Archean|Of the Talga Talga Subgroup (Warrawoona Group). Basalts and cherts. Overlies the McPhee Formation. Age: 3469+/-3Ma (Nelson 1999). See also Mount Ada Formation. Mount is Mt in text.||||||07-FEB-11
26045|Mount Ada Basalt|31309|2|Defined|p53|Archean|Archean|||||||07-NOV-08
26045|Mount Ada Basalt|38498|5|Briefly described|Table 1|||||||||
26045|Mount Ada Basalt|38510|6|Mentioned|Fig.1|||||||||
26045|Mount Ada Basalt|38544|6|Mentioned|Fig.1|||||||||
26045|Mount Ada Basalt|39672|6|Mentioned|Fig.2|||||||||
26045|Mount Ada Basalt|39697|3|Fully described|p91|||||||||
26045|Mount Ada Basalt|40596|6|Mentioned|Fig.1|||||||||
26045|Mount Ada Basalt|41029|5|Briefly described|p106|||||||||
26045|Mount Ada Basalt|41624|6|Mentioned|p44|||||||||
26045|Mount Ada Basalt|43595|6|Mentioned|Table 2-28,p214|||||||||
26045|Mount Ada Basalt|43698|6|Mentioned|p9|||||||||
26045|Mount Ada Basalt|43769|6|Mentioned|p858|||||||||
26045|Mount Ada Basalt|44150|5|Briefly described|p129, p132 Fig.2-131, p133 Tb.2-16|||See also p137-9, p152 Tb.2-22, p157 Fig.2-144. Up to 2.5km thick. Appears as Mount Ada Formation in Fig.2-131, and as Mount Ida Basalt on p157. Formerly part of Friendly Creek Formation (of Fitton et al., 1975) and part of Sharks Formation (Ingram, 1977).||Talga Talga Subgroup|||Metabasalt (pillowed or massive) with dolerite sills, local carbonate alteration; minor chert; local chert, black shale, felsic tuff.|
26045|Mount Ada Basalt|44229|5|Briefly described|Map Legend|Archean|Archean|Of the Talga Talga Subgroup (Warrawoona Group).  Fine-grained amphibolite (after basalt) and siliceous metabasalt; minor metachert and ultramafic rock.||||||07-NOV-08
26045|Mount Ada Basalt|46922|6|Mentioned|p259|||Trace element analysis.||||||
26045|Mount Ada Basalt|50189|4|Described|p7|Archean|Archean|Of the Talga Talga Subgroup. Massive metabasalts of blue-grey to dark-green-grey, fine grained, actinolite-rich rocks with chlorite, epidote and plagioclase. Age: >3471Ma. Discordantly intruded by the Coppin Gap Granodiorite.||||||07-NOV-08
26045|Mount Ada Basalt|50381|5|Briefly described|Map Legend|Archean|Archean|Of Talga Talga Subgroup (Warrawoona Group) Geological Province: Pilbara Craton.||||||07-NOV-08
26045|Mount Ada Basalt|50427|5|Briefly described|p192 Fig.11|Archean|Archean|Written Mt in text.||||||07-NOV-08
26045|Mount Ada Basalt|50544|3|Fully described|p20, p21 Tb. 4|Archean|Archean|Of the Warrawoona Group.  Massive tholeiitic basalt, minor serpentine, chert.  Upper parts overlie and interlayer with Duffer Formation.  Intruded by Coppin Gap Granodiorite and Munganbrina Monzogranite.  Max. thickness:  ~2000m.||||||07-NOV-08
26045|Mount Ada Basalt|50555|5|Briefly described|Map legend|Archean|Archean|Of the Talga Talga Subgroup (Warrawoona Group). Fine-grained amphibolite (after basalt) and siliceous metabasalt.  Geological Province: Pilbara Craton.||||||07-NOV-08
26045|Mount Ada Basalt|60112|5|Briefly described|p108, p109 Fig.2. |||||Unit in Warrawoona Group.||Overlies the Double Bar Formation. Is overlain by Duffer Formation.||
26045|Mount Ada Basalt|60429|4|Described|p7|Archean|Archean|Of Talga Talga Subgroup (Warrawoona Gp). Age:>3471Ma. Disconformable below Duffer Fm. Max. thick: >2000m. Intruded by Coppin Gap Granodiorite. Metabasalts + abundant minor chlorite, epidote and plagioclase; quartz is minor, opaque minerals are accessory.||||||07-FEB-11
26045|Mount Ada Basalt|60636|5|Briefly described|p38|Archean|Archean|Mainly basalt. Underlies the Duffer Formation. Name used interchangeably with Mount Ada Formation.||||||07-FEB-11
26045|Mount Ada Basalt|61253|5|Briefly described| p52 Fig. 2|Archean|Archean|Geological Province: eastern Pilbara Craton.||||||07-NOV-08
26045|Mount Ada Basalt|61257|5|Briefly described|p354 Fig. 1|Archean|Archean|Geological Province: North Pole Dome of the Pilbara Craton.  Mount is Mt in text of figure.||||||07-NOV-08
26045|Mount Ada Basalt|61266|4|Described|p58 Tb.1|Archean|Archean|Of the Talga Talga Subgroup. (Warrawoona Group). Basalts and chert. Age: >3471 Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
26045|Mount Ada Basalt|61579|5|Briefly described|p58 Fig. 2|Archean|Archean|Of the Warrawoona Group.||||||07-NOV-08
26045|Mount Ada Basalt|62427|6|Mentioned|p4, p15|||||||Is overlain by Duffer Formation.||
26045|Mount Ada Basalt|62979|5|Briefly described|p212 Fig. 1, p213|Archean|Archean|Of the Warrawoona Group. Age: 3469Ma. Mount is sometimes Mt in text. Geological Province: Pilbara Craton.||||||07-FEB-11
26045|Mount Ada Basalt|63245|5|Briefly described|p5 Fig. 2|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Age: 3468Ma. Geological Province: Pilbara Craton. Includes a thin chert layer with putative microfossils. Mount is Mt in text.||||||07-NOV-08
26045|Mount Ada Basalt|63417|5|Briefly described|Map legend|Archean|Archean|Of the Coongan Subgroup (Warrawoona Group, Pilbara Supergroup). Geological Province: Pilbara Craton. Mafic volcanic rocks; local ultramafic rocks; metamorphosed.||||||07-NOV-08
26045|Mount Ada Basalt|63420|5|Briefly described|Map legend|Archean|Archean|Of Coongan Subgroup (Warrawoona Group, Pilbara Supergroup). Age: c.3469Ma. Geological Province: Pilbara Craton. Mafic volcanic rock; local ultramafic rock; metamorphosed (detailed lithology included).||||||07-NOV-08
26045|Mount Ada Basalt|63441|5|Briefly described|p4 Tb. 1|Archean|Archean|Of Coongan Subgroup (Warrawoona Group, Pilbara Supergroup).||||||07-FEB-11
26045|Mount Ada Basalt|63538|4|Described|p3 Fig. 2, p8 Tb. 1, p8, p13, p9 Fig. 3|Archean|Archean|Of Coongan Subgroup (Warrawoona Group). Underlies Duffer Formation conformably. Geological Province: Pilbara Craton. Basalts that vary from massive to either highly vesicular of highly variolitic.||||||17-APR-13
26045|Mount Ada Basalt|63649|6|Mentioned|p202 Fig. 3|||Geological Province: Pilbara Craton. Mount is Mt in text of figure.||||||07-FEB-11
26045|Mount Ada Basalt|64328|5|Briefly described|p56 Tb. 1|||Of Talga Talga Subgroup (Warrawoona Group). Basalt.||||||07-FEB-11
26045|Mount Ada Basalt|64405|5|Briefly described|p4 Fig. 3|Archean|Archean|Name inferred from Mt Ada only in Figure 3. Of the Warrawoona Group (De Grey Supergroup). Mount is Mt in text of figure.||||||07-FEB-11
26045|Mount Ada Basalt|64621|5|Briefly described|Map legend|Archean|Archean|Of the Coongan Subgroup (Warrawoona Group). Contains the Antarctic Creek Member.  Lithological details included.||||||07-NOV-08
26045|Mount Ada Basalt|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Talga Talga Subgroup (Warrawoona Group). Geological Province: Pilbara Craton. Undivided metamorphosed mafic volcanic and sedimentary rocks.||||||07-FEB-11
26045|Mount Ada Basalt|64747|6|Mentioned|p120||||||Includes Antarctic Creek Member.|||
26045|Mount Ada Basalt|64936|5|Briefly described|map legend|Archean|Archean|Of Talga Talga Subgroup. Over McPhee Formation; under Duffer Formation. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
26045|Mount Ada Basalt|65008|5|Briefly described|p9, p41|||East Pilbara Granite-Greenstone Terrane.||Of the Talga Talga Subgroup|||Undivided metamorphosed mafic volcanic and sedimentary rocks.|
26045|Mount Ada Basalt|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.|c.3469 Ma (Nelson 1999).|Of Talga Talga Subgroup. |||Mapped as two sub-units: serpentine-talc-chlorite rock after peridotite; fine-grained amphibolite, silicified metabasalt, minor metachert.|
26045|Mount Ada Basalt|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c.3469 Ma.|Of Coongan Subgroup. |||Fine-grained amphibolite, locally schistose; metamorphosed basalt; includes minor metachert and metamorphosed ultramafic rocks; serpentinized komatiite and peridotite, includes talc-serpentine-tremolite-carbonate rock.|
26045|Mount Ada Basalt|65757|6|Mentioned|p81 Tb. 2|||Includes Antarctic Creek Member. Part of the Warrawoona Group, written Mt in text.||||||
26045|Mount Ada Basalt|65827|3|Fully described|p12 Tb.3, p17, p25|Paleoarchean|Paleoarchean|3469 +/- 3 Ma SHRIMP U-Pb zircon; Nelson (1999). Of Coongan Subgroup; formerly of Talga Talga Subgroup.  Underlies Duffer Formation; overlies older greenstones; intruded by Munganbrina Monzogranite and Coppin Gap Granodiorite. Massive fine-grained amphibolite (after basalt), siliceous metabasalt and minor metamorphosed chert.||||||
26045|Mount Ada Basalt|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Coongan Subgroup. Mafic volcanic rocks; local ultramafic rocks; metamorphosed. Includes two mapped but unnamed units; arenite and multi-coloured chert, some beds with impact spherules; and interlayered amphibolite with granite and pegmatite veins.||||||
26045|Mount Ada Basalt|66217|3|Fully described|p5, pp15-19, p59, p60.|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. 2000 to 2500 m thick. Type area extends 3 km NW from McPhee Reward mine. Greenschist facies. Local stromatolites resemble those in the Dresser Formation. Contact metamorphosed by Muccan and Mount Edgar Granitic Complexes. Hosts the Farrel Well Cu-Ni occurrence.|3469 +/- 3 Ma (Nelson 1999b).|Unit in Coongan Subgroup.||Conformably overlies McPhee and Dresser Formations.  Is intruded by Apex Basalt feeder dykes. Is conformably overlain by, and interfingers with, Duffer Formation.|Dominantly pillowed metabasalt, metamorphosed pyroxene spinifex-textured komatiitic basalt, and thin horizons of metasedimentary chert and felsic volcaniclastic rocks; numerous dolerite and gabbro sills.|
26045|Mount Ada Basalt|66664|5|Briefly described|p4, p5, p6. |||||Unit in Warrawoona Group.|||Basalt and chert.|
26045|Mount Ada Basalt|66745|3|Fully described|pp53-54, p57.|Paleoarchean|Paleoarchean|Deepening of depositional basins.|c.3470 Ma.|Unit in Coongan Subgroup.||Disconformably overlies Dresser and McPhee Formations. Is overlain by Duffer Formation.|Basalt; minor komatiitic basalt, jaspilite, felsic volcanic rocks.|
26045|Mount Ada Basalt|67130|5|Briefly described|p13, p63, p69,  p75|Paleoarchean|Paleoarchean|At least 150m thick.|3474 Ma - 3463 Ma|Warrawoona Group|Includes Antarctic Creek Member|Overlies Dresser Formation, McPhee Formation, disconformably overlain by Duffer Formation, Unconformably overlain by Strelley Pool Formation|Basalt, layered red and black chert.|
26045|Mount Ada Basalt|67197|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Coongan Subgroup.||||
26045|Mount Ada Basalt|67201|5|Briefly described|p7 Fig.4, p12 Tb.1|||In northern Pilbara Craton, East Pilbara Terrane. Shown as Mt Ada Basalt.||Coongan Subgroup||||
26045|Mount Ada Basalt|67269|5|Briefly described|p5, p6-9, p12-14|Paleoarchean|Paleoarchean||c.3470 Ma.|Warrawoona Group.|Antarctic Creek Member.|Overlies Dresser Formation, and locally the Mount Ada Basalt unconformably. Is overlain by Duffer Formation and locally unconformably by Panorama Formation.|Carbonate-altered pillow metabasalt; pyrophyllite-altered schistose metabasalt.|
26045|Mount Ada Basalt|67270|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.|c.3470 Ma.|Coongan Subgroup.||||
26045|Mount Ada Basalt|67668|6|Mentioned|Fig. 2; p. 153||Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Warrawoona Group||Underlies the Duffer Formation and Marble Bar Chert, overlies the Dresser and McPhee Formations|Mafic volcanic rocks.|
26045|Mount Ada Basalt|68035|4|Described|p288 Fig 4|Paleoarchean|Paleoarchean|Warrawoona Group, Pilbara Supergroup, East Pilbara Terrane.|~3470 Ma|Of Coongan Subgroup.||Overlain by and in part laterally equivalent to Duffer Formation.|Basalt with minor felsic volcanics, siliciclastic rocks, jaspilite, komatiitic basalt.|
26045|Mount Ada Basalt|68280|5|Briefly described|p2, p4, p11, p22 fig 19||||c. 3470 Ma|Coongan Subgroup|Includes Antarctic Creek Member|Disconformably overlies Dresser Formation, McPhee Formation, overlain by Duffer Formation, unconformably overlain by Strelley Pool Formation|Basalt and felsic volcanic rocks, komatiitic basalt, siliciclastic rocks and jaspilite.|
26045|Mount Ada Basalt|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Coongan Subgroup|||Mafic schist derived from komatiitic basalt; tremolite-chlorite-serpentine and chlorite-carbonate schist; chert, metamorphosed.|23-SEP-13
26045|Mount Ada Basalt|68283|5|Briefly described|Map Legend|Archean|Archean|East Pilbara Terrane, Pilbara Craton. The 5 facies are mapped separately.||Of the Coongan Subgroup.|||Mafic volcanic rock, local ultramafic rock, metamorphosed; strongly foliated to schistose amphibolite; serpentinized komatiite and peridotite; komatiitic basalt, massive and pillowed, local spinifex texture, metamorphosed; chert, metamorphosed.|23-SEP-13
26045|Mount Ada Basalt|68284|5|Briefly described|p5, 7|Paleoarchean|Paleoarchean|Allwood et al. (2007). East Pilbara Terrane, Pilbara Craton.|c.3470 Ma.|Coongan Subgroup (Warrawoona Group).||Overlies McPhee and Dresser Formations. Is overlain by Duffer Formation; locally by Strelley Pool Formation.||
26045|Mount Ada Basalt|69012|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane. The five facies are mapped separately.|3470-3469 Ma|Of the Coongan Subgroup.|||Basalt, locally massive but generally pillowed, local dolerite sills; pillow basalt; komatiitic basalt with local pyroxene spinifex texture; dolerite and local gabbro; chert: all metamorphosed.|28-APR-14
26045|Mount Ada Basalt|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Also includes 8 unnamed sub-units mapped separately. See map legend for a detailed lithology. Age range constrained by surrounding rock units.|3477-3449 Ma|Of the Coongan Subgroup.|Includes the Antarctic Creek Member.||Metamafic volcanic rock; amphibolite; carbonate-altered metabasalt; silicified metamafic volcanic rock; chert; felsic volaniclastic and carbonate rocks; arenite; dolerite and local gabbro; pillow basalt; komatiitic basalt.|02-MAY-14
26045|Mount Ada Basalt|69041|4|Described|p12|Archaean|Archaean|Defined and described by Hickan (1977). |>3471 Ma (Williams, 1998)|||Intruded by the Coppin Gap Suite. Disconformably overlain by the Duffer Formation.|Fine-grained and comprises amphibolite (after basalt) and siliceous meta-basalt, minor metachert, and ultramafic rocks.Metabasalts are blue-grey to dark green, fine-grained, actinolite rich rocks with chlorite, epidote and plagioclase.|
26045|Mount Ada Basalt|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Interlayered amphibolite and metamorphosed granitic rocks, metamafic volcanic rock. Age derived from felsic volcanic granophyre sample (142976.1.pdf)|3469 Ma +/- 3 Ma (SHRIMP)|Talga Talga Subgroup|Includes Antarctic Creek Member|Overlain by Duffer Formation|Dacitic volcaniclastic rock; tuffaceous, with accretionary lapilli; metamorphosed.  Metabasalt, komatiitic basalt; metamorphosed, mafic and ultramafic schists, serpentinized komatiite and peridotite and metachert.|
26045|Mount Ada Basalt|69301|4|Described|p5 Fig.3, p9 Tb.1, p11, p20 Tb.2|||Pilbara Craton. East Pilbara Terrane. Shown as Mt Ada Basalt.|c. 3470 Ma|Coongan Subgroup|||Basalt; with jaspilite, siliciclastic rocks, felsic volcanic rocks, komatiitic basalt.|
26045|Mount Ada Basalt|69563|5|Briefly described|p690 Tb.1|||Pilbara Craton.|3470.1 +/- 1.9 Ma.||Includes Antarctic Creek Member.|||
26045|Mount Ada Basalt|69566|6|Mentioned|p236|||East Pilbara Granite-Greenstone Terrane.||Warrawoona Group.||Is overlain by Duffer Formation.||
26045|Mount Ada Basalt|69569|6|Mentioned|p285 Fig.1, p287|||East Pilbara Terrane. Contains an impact spherule bed dated at 3470+/- 2 Ma (Byerly et al., 2002).||Warrawoona Group.||||
26045|Mount Ada Basalt|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. In contact wih a c. 3310+\-3 Ma hornblende granodiorite (Sample GSWA 142974). Sample GSWA 142976 (porphyritic granophyre) yielded an interpreted igneous crystallisation age of 3469+\-3 MA  (weighted mean 207Pb/206Pb). Sample GSWA 148500 (lapilli tuff interbedded in Mount Ada Basalt) yielded an interpreted igneous crystallisation age of 3469+\-3 Ma for the tuff (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.|3477-3469 Ma (inferred)|Unit of Coongan Subgroup.|Includes Antarctic Creek Member.|Overlain by Duffer Formation.|Amphibolite; komatiitic, pillowed and variolitic basalt, carboante-altered mafic and ultramafic rocks, chert, dacitic volcaniclastics; dolerite and gabbro, serpentinised komatiite and peridotite, ultramafic schist.|
26045|Mount Ada Basalt|70022|6|Mentioned|p115|||East Pilbara Terrane.||Coongan Subgroup.||||
26045|Mount Ada Basalt|70507|5|Briefly described|p431|Archean|Archean|Geological province: Pilbara Craton.||Unit of Pilbara Supergroup.||||
26045|Mount Ada Basalt|70733|6|Mentioned|p103|||Pilbara Craton.|||Antarctic Creek Member.|||
26045|Mount Ada Basalt|70775|5|Briefly described|p12|||East Pilbara.||Warrawoona Group||Overlies the Dresser and McPhee Formations. Overlain by the Duffer Formation.||
26045|Mount Ada Basalt|70834|6|Mentioned|p298|Paleoarchean|Paleoarchean|Marble Bar greenstone belt, Pilbara Craton.|3469 Ma.|||Overlies McPhee Formation. Is overlain by Duffer Formation.||
26045|Mount Ada Basalt|70884|4|Described|p123-126,128-131,133-134,136-137|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Depositional environment: low-energy, deep marine, proximal to volcanic sources. Earliest exposed rocks within the Doolena Gap Greenstone Belt. ~500m thick succession exposed almost continuously in the Low-Strain Belt. Carbonate alteration observed within the basaltic rocks in shear zones in the Low-Strain Belt. Layer-parallel and discordant mafic bodies, increasing in frequency downwards stratigraphically, interpreted as sills and dykes that represent intracrustal feeder systems (evidence from developent of f1a listric faults) to the supracrustal pillow flows. |c. 3.47 Ga|Unit of Coongan Subgroup.||Overlain by Duffer Formation. Underlain by Mc Phee Formation/Talga Talga Subgroup.|(Meta-)basalts, mafic intrusions (gabbro, dolerite, pyroxenite), anorthosite, chert/BIFs, (Meta-)siltstones, pumiceous stuff, chrolite-quartz schist.|
26045|Mount Ada Basalt|71137|6|Mentioned|p15|Archean|Archean|East Pilbara region. Associated with a locality containing microfossils having some similarities with those in the Farrel Quartzite.|3.5 Ga (van Kranendonk, 2006).|||||
26045|Mount Ada Basalt|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Warrawoona  Large Igneous Province.|max age 3470+/-1 Ma, min 3469+/-3 Ma.|Coongan Subgroup|||Mafic volcanic rock; local ultramafic rock; metamorphosed.|
26045|Mount Ada Basalt|72064|5|Briefly described|p66|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawoona Group.||Overlain by Duffer Formation. Underlain unconformably by McPhee Formation.||
26045|Mount Ada Basalt|72251|5|Briefly described|p54|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Coongan Subgroup.||Lower unit of Coongan Subgroup. Overlain by Duffer Formation. Underlain by McPhee and Dresser Formations.||
26045|Mount Ada Basalt|72668|6|Mentioned|p4-6, p11, p18, p22|||East Pilbara Terrane. Marble Bar greenstone belt, North Pole Dome.|c. 3470 Ma|Coongan Subgroup||Unconformably overlain by Kelly Group. Overlain by the Duffer Formation.||13-JAN-22
26045|Mount Ada Basalt|73160|4|Described|p2 Fig.1, p3-4, p5 Fig.3, p12-14|Paleoarchean|Paleoarchean|Pilbara Craton. Prehnite-pumpellyyite assemblages restricted to upper portion. Lower and upper parts shown on p2 Fig.1, separated in places by a spherulitic chert. Location in text includes p8 Fig.6.|~3470 Ma|Warrawoona Group||Overlies Dresser Formation.|Pillow basalt, hosts minor doleritic intrusions.|
26045|Mount Ada Basalt|73598|6|Mentioned|p1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Coongan Subgroup.||Overlies McPhee and Dresser Formations. Is overlain by Duffer Formation.||
22396|Mount Aloysius Complex|44109|3|Fully described|p26-39, p136|Mesoproterozoic|Mesoproterozoic|Felsic granulite; derived from igenous protoliths; mafic granulite layers and lenses; metasedimentary rocks, including quartzite, metapelite and calc-silicate granulite, orthogneiss, syenite.||||||
22396|Mount Aloysius Complex|61339|5|Briefly described|Map legend|||||||||
22396|Mount Aloysius Complex|69153|6|Mentioned|GA_geochron.csv|||25 samples described. 23 samples refer to: Sun, S.S. Gray, C.M. Sheraton, J.W. 1995. Zircon U-Pb chronology and neodymium isotope study of tectono-thermal and crustal forming events in the Tomkinson Ranges, western Musgrave Block, Central Australia.|||||Felsic gneiss, felsic and intermediate and mafic intrusives, metasediment; granite, gabbronorite dyke, quartz monzodiorite, quartz monzodiorite and pelite.|
22396|Mount Aloysius Complex|70634|5|Briefly described|GA_geochron.csv|Paleoproterozoic|Paleoproterozoic|Sample Descriptions: BT granite augen gneiss (rapakivi), GNT-PL-QZ-KFS gneiss, porphyritic BT-HBL quartz monzonite (rapakivi), OPX-BT-CPX quartz monzodiorite|1901 Ma - 2118 Ma (Sm-Nd)|||||
22396|Mount Aloysius Complex|71592|5|Briefly described|Appendix A.|||Musgrave Province. Metamorphosed at 1223 +/- 7 Ma (U-Pb zircon SHRIMP).|1305+/-8 Ma (crystallisation: U-Pb zircon SHRIMP)||||Gneiss.|
27203|Mount Augustus Sandstone|22905|6|Mentioned|p52 Fig. 2|||Of the Edmund Subgroup (Bangemall Group).  Mount as Mt. in text.||||||24-JAN-06
27203|Mount Augustus Sandstone|23280|6|Mentioned|Table1p1085|||Written: Mt Augustus Sandstone.||||||
27203|Mount Augustus Sandstone|23310|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of Bangemall Group.||||||
27203|Mount Augustus Sandstone|23723|6|Mentioned|p9|||Geological Province: Bangemall Basin.||||||
27203|Mount Augustus Sandstone|24183|5|Briefly described|p4 Fig.3|||Of the Edmund Subgroup (Muhling and Brakel, 1985)||||||
27203|Mount Augustus Sandstone|24544|5|Briefly described|p43|||Pebbly sandstone. Previously of the Edmund Subgroup, correlation now uncertain.||||||24-FEB-05
27203|Mount Augustus Sandstone|29916|4|Described|p115|||||||||
27203|Mount Augustus Sandstone|36551|6|Mentioned|p101|||||||||
27203|Mount Augustus Sandstone|37460|4|Described|p160|||||||||
27203|Mount Augustus Sandstone|39370|4|Described|p31|||||||||
27203|Mount Augustus Sandstone|40089|2|Defined|p17|Mesoproterozoic|Mesoproterozoic|||||||
27203|Mount Augustus Sandstone|40899|6|Mentioned|Fig.1|||||||||
27203|Mount Augustus Sandstone|41360|6|Mentioned|p191|||||||||
27203|Mount Augustus Sandstone|44142|5|Briefly described|p314 Tb.4-4, p311, p317, p321|||200-400m thick alluvial fan deposits overlying Gascoyne Complex. Restricted area. ||Basal unit in Edmund Subgroup.||Correlated with Tringadee Formation.|Coarse-grained sandstone, scattered pebbles; minor conglomerate.|
27203|Mount Augustus Sandstone|50225|5|Briefly described|p387 Fig. 2|||Formerly of the Edmund Subgroup (Bangemall Group) - now superseded and reassigned to Tringadee Formation?  Mount is Mt. in text.||||||07-FEB-11
27203|Mount Augustus Sandstone|63470|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Augustus Basin. Sandstone, pebbly sandstone and conglomerate; minor siltstone.||||||07-NOV-08
27203|Mount Augustus Sandstone|63471|5|Briefly described|Map legend||Paleoproterozoic|Geological Province: Mount Augustus Basin. Sandstone, pebbly sandstone and conglomerate; minor siltstone.||||||07-NOV-08
27203|Mount Augustus Sandstone|64580|4|Described|map legend||Mesoproterozoic|Sandstone, pebbly sandstone and conglomerate; minor siltstone.||||||09-DEC-08
27203|Mount Augustus Sandstone|64728|5|Briefly described|p95 Fig.2, pp98-100, p107.|||Fluvial. Highly variable paleocurrent directions.|Contains detrital zircons, c.1800 and c.1680 Ma.|||A correlative of Yilgatherra Formation.|Coarse-grained, feldspathic sandstone.|
27203|Mount Augustus Sandstone|65450|6|Mentioned|p2 Fig.1, p6 Fig.4|||Shown as Mt Augustus Sandstone.||||||
27203|Mount Augustus Sandstone|65453|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Faulted against Edmund Group; overlies Moorarie Supersuite. Sandstone, pebbly sandstone, and conglomerate; minor siltstone. Geol. Prov: Mount Augustus Basin.||||||
27203|Mount Augustus Sandstone|65830|4|Described|p4, p5, p19-21; Plates 1,2|Calymmian|Statherian|Over 1150m thick. Localised fluvial deposit. Either a thickened correlative of the lower Yilgatherra Formation, or a correlative of the Bresnahan Group.||||Unconformably overlies Gascoyne Complex. ?Conformably overlain by the Irregully Formation. ?Correlative of the Yilgatherra Formation. ?Faulted contact with the Pooranoo Metamorphics.|Upward fining succession varying from localised pebble to boulder conglomerate, through very coarse grained sandstone, to fine-grained sandstone (largely feldspathic and tourmaline-bearing).|
27203|Mount Augustus Sandstone|66105|5|Briefly described|Map legend|Proterozoic|Proterozoic|Mount Augustus Basin. Sandstone, pebbly sandstone, and conglomerate; minor siltstone. Includes a mapped but unnamed unit of sandstone, minor pebbly sandstone, siltstone and conglomerate.||||||
27203|Mount Augustus Sandstone|66299|5|Briefly described|p4 Fig.2, p155, p159.|Mesoproterozoic|Mesoproterozoic||c.1620 Ma.|||Unconformably overlies Leake Spring Metamorphics and units of Moorarie Supersuite.||
27203|Mount Augustus Sandstone|66887|5|Briefly described|p3 Fig.2, p7|Mesoproterozoic|Mesoproterozoic|Southern Gascoyne Province.||Edmund Group|Overlies Halfway Gneiss in Limejuice Zone|||
27203|Mount Augustus Sandstone|67246|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic||||||Sandstone; minor pebbly sandstone, siltstone and conglomerate.|19-NOV-13
27203|Mount Augustus Sandstone|67346|6|Mentioned|p794 Fig.1, p796 Fig.3|||Mount is spelt Mt in text.||||||11-MAY-12
27203|Mount Augustus Sandstone|67843|6|Mentioned|p2 Fig.1. |Mesoproterozoic|Mesoproterozoic|||||||
27203|Mount Augustus Sandstone|69003|5|Briefly described|p4, p35|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen. Fluvial sediments. Locally preserved. May correlate with basal Edmund Group; alternatively may be an older, unrelated unit.||||||
27203|Mount Augustus Sandstone|69028|5|Briefly described|Map Legend|Calymmian|Statherian|Mount Augustus Basin.|1620-1465 Ma||||Sandstone, pebbly sandstone, and conglomerate; minor siltstone.|06-MAY-14
27203|Mount Augustus Sandstone|69080|5|Briefly described|p684, p692 Fig.7, p697 Fig.11|||Gascoyne Province.|||||Sandstone; minor pebbly sandstone, siltstone and conglomerate.|
27203|Mount Augustus Sandstone|69166|5|Briefly described|geologyp_lut.csv|Mesoproterozoic|Paleoproterozoic|Age derived from feldspathic sandstone sample (148972.1.pdf) May correlate with locally preserved fluvial facies of Yilgatherra Formation|1664 Ma +/- 6 Ma (SHRIMP)||||Conglomerate, sandstone, pebbly sandstone,conglomerate and minor siltstone|
27203|Mount Augustus Sandstone|69387|6|Mentioned|p18|||Limejuice Zone, Gascoyne Province. Structural interpretation diagram.||||||
27203|Mount Augustus Sandstone|70019|5|Briefly described|p91,93,108,109||Paleoproterozoic|Geological province: Gascoyne Province, Capricorn Orogen. Detrital zircons reflect the age of the underlying granitic rocks of the Gascoyne Province; youngest population dated at c. 1680 Ma (Martin et al., 2008). Maximum depositional age of Edmund Group is constrained by 1679+\-3 Ma detrital zircons from the Mt Augustus Sandstone.||Unit of Yilgatherra Formation.||Overlain by Yilgatherra Formation. Underlain by Paleoproterozoic basement.||
27203|Mount Augustus Sandstone|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 2_5m_interpgeop15_lut.csv, 500k_interpgeop14_lut.csv, 149029.1.pdf, West Australian Craton, Mount Augustus Basin|1685-1610 Ma|||May correlate with fluvial facies at the base of the Yilgatherra Formation, Overlain by Yilgatherra Formation|Sandstone, Feldspathic sandstone, conglomerate, pebbly sandstone; minor siltstone.|
27203|Mount Augustus Sandstone|70814|5|Briefly described|p3, p8, p17, p31, p39|||Edmund Basin. Contains detrital zircons as young as c. 1679 Ma. Note that the contact between this formation and the Edmund Group is either faulted or not exposed.||||Unconformably overlain by (or faulted against) the Yilgatherra or Irregully Formations.||
27203|Mount Augustus Sandstone|70826|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|||||||
27203|Mount Augustus Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, siltstone, sandstone|
27203|Mount Augustus Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Mount Augustus Basin.|||||Sandstone, pebbly sandstone, and conglomerate; minor siltstone.|
27203|Mount Augustus Sandstone|72259|6|Mentioned|p3|Calymmian|Statherian|||||||
27203|Mount Augustus Sandstone|72705|5|Briefly described|p5, 9, 11|Mesoproterozoic|Mesoproterozoic|||||Correlative of Yilgatherra Formation.||
27203|Mount Augustus Sandstone|73102|5|Briefly described|p3|||Gascoyne Province.|||||Sandstone; minor pebbly sandstone, siltstone, and conglomerate.|
27203|Mount Augustus Sandstone|73214|6|Mentioned|p974 Fig.1|Mesoproterozoic|Mesoproterozoic|||||||
27203|Mount Augustus Sandstone|73442|5|Briefly described|p3|||Gascoyne Province.|||||Sandstone, minor pebbly sandstone, siltstone, and conglomerate.|
27840|Mount Barren Group|9173|5|Briefly described|Map legend.|Proterozoic|Proterozoic||||Includes Kybulup Schist and Kundip Quartzite.|||
27840|Mount Barren Group|22493|6|Mentioned|p102|||Mount is written MT in text||||||
27840|Mount Barren Group|22635|6|Mentioned|p493||Proterozoic|Mount spelled Mt in text||||||
27840|Mount Barren Group|22716|5|Briefly described|table4, p238|Mesoproterozoic|Mesoproterozoic|||||||
27840|Mount Barren Group|22790|5|Briefly described|p52|||||||||
27840|Mount Barren Group|23514|5|Briefly described|p102 Fig.1|Mesoproterozoic|Mesoproterozoic|||||||
27840|Mount Barren Group|23727|5|Briefly described|p71|Mesoproterozoic|Mesoproterozoic|Age: 1700-1300 Ma.||||||
27840|Mount Barren Group|23728|5|Briefly described|Map Legend|Proterozoic||Geological Province Albany-Fraser Orogen.||||||
27840|Mount Barren Group|23752|4|Described|p13|Proterozoic|Proterozoic|Age: ~1550-1300 Ma.||||||
27840|Mount Barren Group|23753|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes Steere Formation, Kundip Quartzite and Kybulup Schist.  Geological Province: Albany-Fraser Orogen.||||||30-NOV-09
27840|Mount Barren Group|23754|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province Albany-Fraser Orogen.||||||
27840|Mount Barren Group|23808|5|Briefly described|p2|Neoproterozoic|Neoproterozoic|Geological Province: Yilgarn Craton.||||||
27840|Mount Barren Group|24160|6|Mentioned|p150, p151 Fig.76.|||Northern foreland of Albany-Fraser Orogen.||||||
27840|Mount Barren Group|24165|5|Briefly described|p13, p31, p57, p93|Mesoproterozoic|Paleoproterozoic|Albany-Fraser Orogen. Features imbricate thrusting. Recently recognised as prospective for gold mineralisation. Hosts base metal mineralisation at Trilogy prospect. Moderate potential for nickel sulfides.|||||Psammitic and subordinate pelitic metasedimentary rocks: shale, sandstone, phyllite and schist; quartzite and dolomite.|
27840|Mount Barren Group|24526|6|Mentioned|p105 Fig. 6|Paleoproterozoic||Max. ages: 1851+/-30, 2634+/-14 and 2726+/-44Ma (Nelson 1996). Geological Province: Yilgarn Craton.||||||07-NOV-08
27840|Mount Barren Group|24542|6|Mentioned|p2 Fig.2|Proterozoic|Proterozoic|||||||
27840|Mount Barren Group|38764|4|Described|p109|||||||||
27840|Mount Barren Group|41341|5|Briefly described|p8|||||||||
27840|Mount Barren Group|41842|6|Mentioned|p57|||||||||
27840|Mount Barren Group|42023|6|Mentioned|p159|||See also Fig.2||||||
27840|Mount Barren Group|42424|5|Briefly described|p3|||||||||
27840|Mount Barren Group|42890|5|Briefly described|p294|||Actually spelt Mt Barren Group.||||||21-OCT-08
27840|Mount Barren Group|43012|5|Briefly described|p168|||||||||
27840|Mount Barren Group|43030|5|Briefly described|Map Legend|||||||||
27840|Mount Barren Group|43038|6|Mentioned|p9|||||||||
27840|Mount Barren Group|43189|5|Briefly described|Map Legend||Proterozoic|||||||
27840|Mount Barren Group|43203|5|Briefly described|Map Legend||Proterozoic|||||||
27840|Mount Barren Group|43212|5|Briefly described|p1,p4.|||||||||
27840|Mount Barren Group|43498|4|Described|2,6|||||||||
27840|Mount Barren Group|43573|6|Mentioned|p314||Proterozoic|||||||
27840|Mount Barren Group|44137|5|Briefly described|p255; p256-259 Figs.3-42,-43,-45,-46;|||Defined by Thom and Chin (1984); comprises 3 Formations. Strongly deformed to S and W of Albany Orogen; appears to be allochthonous. Folding and refolding on all scales throughout.|||Includes Steere Formation, Kundip Quartzite, Kybulup Schist.|||30-APR-15
27840|Mount Barren Group|50011|5|Briefly described|p63|Paleoproterozoic|Paleoproterozoic|Age: 1696 +/- 7Ma. Geological Province: Albany-Fraser Orogen.||||||07-NOV-08
27840|Mount Barren Group|60555|5|Briefly described|p4 Tb. 1, p13|Mesoproterozoic|Proterozoic|Age: 1205+/-10Ma (Dawson et al., 2003) and 1696+/-7Ma (Dawson et al., 2002).||||||30-NOV-09
27840|Mount Barren Group|62093|6|Mentioned|p216 Tb. 1|||||||||
27840|Mount Barren Group|62381|4|Described|p2 Fig.2, pp12-17.|||Northern Foreland, Albany-Fraser Orogen. Detrital zircon evidence indicates source(s) other than Yilgarn Craton. Cut by northwest-transporting thrust faults. Southern edge marked by Jerdacuttup Fault.|c.1790 Ma to c.1700 Ma.||Includes basal Steere Formation, Kundip Quartzite and Kybulup Schist.|Locally intruded by Cowerdup Sill.|Quartzite, psammitic to pelitic schist; subordinate dolomite and metaconglomerate.|
27840|Mount Barren Group|63866|4|Described|p183-p185, p187, p193, p197|Proterozoic|Proterozoic|Northern Foreland and Albany-Fraser Belt. Detrital zircon populations found in this group indicates that it must have been derived from sources older than the Yilgarn Craton.|||Includes the Kundip Quartzite and Kybulup Schist.||Conglomerates, sandstones, pelites and stromatolitic carbonates.|
27840|Mount Barren Group|64161|5|Briefly described|p578-581, p591-594|Statherian|Statherian|SHRIMP dating of diagenetic xenotime gives minimum depositional age of 1696 +/- 7 Ma. Possible equivalent of Woodline Formation.|||||Metasediments. Basal conglomerate is partly allochthonous.|21-MAR-12
27840|Mount Barren Group|64340|5|Briefly described|p24, p8 Tb. 1|Proterozoic|Proterozoic|Maximum depositional age: 1696+/-7Ma (Dawson et al., 2002). May be equivalent of Woodline Formation.||||||
27840|Mount Barren Group|64572|6|Mentioned|p796, p811 Fig. 13|Proterozoic|Proterozoic|Siliciclastic sedimentary rocks.||||||22-DEC-08
27840|Mount Barren Group|64577|5|Briefly described|p606 Fig. 1, p607, p616, p618|||Mount is Mt in text. Three metamorphic events identified. Final metamorphic age: 1027+/-8Ma (SHRIMP). Metasediments.||||||10-FEB-14
27840|Mount Barren Group|64580|4|Described|map legend||Paleoproterozoic|Phyllite, pelite and psammite schist; quartzite and metacarbonate.||||||21-OCT-08
27840|Mount Barren Group|64635|6|Mentioned|p2 Fig.1|||||||||
27840|Mount Barren Group|64722|5|Briefly described|Fig. 2 p3-6, p17-18, 19|Statherian|Statherian|Of Northern Foreland, Albany Fraser Orogen. Locally non-conformable on Yilgarn basement. Contains 3160 - 1792 Ma zircons. Age from authigenic xenotime cement.|1693 +/- 4 Ma.||||Conglomerate, quartzite, pelite and stromatolitic carbonates.|11-APR-12
27840|Mount Barren Group|64730|6|Mentioned|p138|Paleoproterozoic|Paleoproterozoic|Southern margin of Yilgarn Craton. Contains sedimentary rocks with 2030-2019 Ma detrital zircons (Nelson 1996; Dawson et al. 2002).||||||03-MAY-12
27840|Mount Barren Group|65260|6|Mentioned|p6 Tb.1, p15|Statherian||1696+/-7 Ma (Dawson et al. 2002); may be a lateral equivalent of Woodline Formation, 400 km to the NE.||||||
27840|Mount Barren Group|65357|5|Briefly described|p330 Fig.1, p335|Statherian|Statherian|Age given as between 1790 Ma (Dawson et al., 2002) and 1694+/-4 (Vallini et al., 2002). May be part of the same basin as the Stirling Range Formation.||||||10-DEC-09
27840|Mount Barren Group|65487|3|Fully described|p15,22-24,2-3,11,55-57,59;Figs.1-2,27-28|Mesoproterozoic|Paleoproterozoic|Partly overlies (thrusted onto) the southern edge of the Yilgarn Craton by Albany-Fraser Orogeny. Lower greenschist-upper amphibolite facies metasediments; deltaic-shallow marine sequence. Divided into Steere Formation, Kundip Quartzite and Kybulup Schist, and hosts the 300 m thick Cowerdup Sill. Age of 1693 +/- 4 Ma (Vallini et al., 2005).||||||10-FEB-14
27840|Mount Barren Group|66302|6|Mentioned|p66||||1696 +/- 7 Ma|||||
27840|Mount Barren Group|67268|6|Mentioned|p4-6, p20|Proterozoic|Proterozoic|Occurs on top of the southern margin of the Yilgarn Craton. Age is maximum depositional age.|c. 1700 Ma (detrital zircon)||Steer Formation, lower, Kundip Quartzite, Kybulup Schist||metasediments|15-JUN-22
27840|Mount Barren Group|67323|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Albany-Fraser Belt. Deposition in an interpreted continental back-arc setting.|~1680-1670 Ma.||||Quartzite, sandstone, dolostone, conglomerate, phyllite, pelitic and psammitic schist.|
27840|Mount Barren Group|67380|6|Mentioned|p6 Fig.3|||Albany-Fraser Orogen.||||||
27840|Mount Barren Group|67722|5|Briefly described|p5 fig 2.2, p7, p8|Statherian|Statherian|Diagenetic xenotime indicates deposition after c.1790 Ma but before c.1700 Ma.|1790-1700 Ma(SHRIMP)||Includes Kybulup Schist, Steere Formation, Kundip Quartzite||Dominated by quartztites, psammites, pelitic schists, dolomites and metaconglomerates.|
27840|Mount Barren Group|67888|6|Mentioned|p68|||||||||
27840|Mount Barren Group|68186|4|Described|p3 Fig.2, p8-11, p13-15, p39, p80|Paleoproterozoic|Paleoproterozoic|Northern Foreland and central Albany-Fraser Orogen. Extends from Bremer Bay to E of Ravensthorpe. Assigned to the newly-named Barren Basin, overlying the Yilgarn Craton. Contained within a separate thrust package between two fault-bound slices of Munglinup Gneiss. Metamorphosed c.1205 Ma.|<c.1700 Ma (maximum depositional age).||Steere Formation, Kundip Quartzite, Kybulup Schist.||Southern part was subject to moderate- to high-strain ductile deformation under amphibolite to granulite facies metamorphism.|
27840|Mount Barren Group|68654|6|Mentioned|p3, p2 Fig 1|Paleoproterozoic|Paleoproterozoic|Barren Basin.|c. 1700 Ma|||||
27840|Mount Barren Group|69003|5|Briefly described|vi, p28, p30, p72|||Barren Basin. Siliciclastic sediments, deposited on the S Yilgarn Craton after c.1800 Ma. Geochronology (U-Pb and diagenetic xenotime) described.|c.1693 Ma.||||Dominantly shallow-marine to fluvial, mature, quartz-rich sandstones with interbedded siltstones and minor conglomerate.|
27840|Mount Barren Group|69252|5|Briefly described|p2, p7 Fig.3, p9-11, p24|Paleoproterozoic|Paleoproterozoic|Fitzgerald River National Park, Albany-Fraser Orogen. A thick (>1.2km) succession of conglomerate, sandstone, mudrock and dolostone; metamorphosed to lower greenschist to upper amphibolite facies at c.1206 Ma to 1194 Ma. Folded and thrust-faulted.|1693 Ma.||Steere Formation, Kundip Quartzite, Kybulup Schist.||Metasedimentary rocks.|
27840|Mount Barren Group|69412|6|Mentioned|p3 Fig.2, p12|||Albany-Fraser Orogen. Paleomagnetic pole c.1300-1050 Ma tabulated.|c.1205 Ma.|||||
27840|Mount Barren Group|69595|5|Briefly described|p3 fig 1, p8, p9 fig 5, p11.|Statherian|Orosirian|Barren Basin, Albany Fraser Orogen.  Interpreted to have been deposited as a deltaic to shallow-marine sequence in a continental rift basin. Significant portions of this unit are made up of c. 1800 Ma detritus. Ages are of detrital zircon components. See also  p13 fig 7a, p15, p17 tbl 3, p19, p35, p36, p38.|1857 - 1773 Ma (GSWA 112168 and 112170)||Steere Formation, Kundip Quartzite, Kybulup Schist.||Lower greenschist to upper amphibolite facies metasedimentary rocks.|
27840|Mount Barren Group|70023|6|Mentioned|p167-p168|||Development of internal fault-bounded successions and fold-thrust sequences during Stage II (c. 1225-1140 Ma) Albany-Fraser Orogeny (Rasmussen et al., 2002; Dawson et al., 2003; Spaggiari et al., 2009, 2011).||||||17-JUL-19
27840|Mount Barren Group|70084|6|Mentioned|p219|Mesoproterozoic|Mesoproterozoic|Geological province: Yilgarn Craton.||||||
27840|Mount Barren Group|70085|6|Mentioned|p233-234, 241|||Barren Basin, Western Albany-Fraser Orogen. Peak metamorphosed c.1205 Ma.||||||
27840|Mount Barren Group|70089|6|Mentioned|p262|||Albany-Fraser Orogen.||||||
27840|Mount Barren Group|70090|4|Described|p442,444,446-447,452-453,456-458|Statherian|Statherian|Geological province: Albany-Fraser Orogen, West Australian Craton. Of Barren Basin. Deposited in a broad, relatively shallow basin under moderate to high-energy, fluvial to shallow marine environments. Contains an overall upward-fining sequence, consistent with a continental rift basin. Maximum depositional age: c.1766 Ma (Recalculated from Dawson et al., 2002; also see Nelson 1996a,d). Minimum depositional age: Deposited by 1693+\-4 Ma (Vallini et al., 2005). Metamorphosed and deformed by Stage II AFO (Dawson et al., 2002; Vallini et al., 2002, 2005). Archean detrital zircon age components include c. 2977, 2715, 2663, and 2645 Ma. Paleoproterozoic components include c. 2450, 2291, 2246, 2018, 1930, 1857, 1803, and 1773 Ma. Zircon ages of 2750-2600 Ma with EHfi array of -5 to 4 corresponds to 3.1 Ga (avg.) model ages.|||Includes Jundip Quartzite, Kybulup Schist and Steere Formation.||Quartz-rich lithologies including cross-bedded sandstones, clean sandstones (now quartzite), pebbly sandstones, and siltstones.|
27840|Mount Barren Group|70182|6|Mentioned|p4-5|Paleoproterozoic|Paleoproterozoic|Barren Basin, Albany-Fraser Orogen.|c.1700 Ma.|||||
27840|Mount Barren Group|70256|6|Mentioned|p3|||Albany-Fraser Orogen.||||||
27840|Mount Barren Group|70802|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Albany-Fraser Orogen. Of Barren Basin. Events: Biranup Orogeny (1710-1620 Ma).|2000-1700 Ma (inferred)||||Phyllite, pelite and psammite schist; quartzite and metacarbonate|
27840|Mount Barren Group|70826|6|Mentioned|p5 tbl 2, p10|Paleoproterozoic|Paleoproterozoic|Mount Barren Basin, Yilgarn Craton.||||||
27840|Mount Barren Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||quartzite, sandstone, crystalline dolostone/dolomite, conglomerate|
27840|Mount Barren Group|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Barren Basin.|||||Phyllite, pelite and psammite schist; quartzite and metacarbonate.|
27840|Mount Barren Group|72059|6|Mentioned|p56|Mesoproterozoic|Mesoproterozoic|Geological province: Fraser Zone, Albany-Fraser Orogen.||||||
27840|Mount Barren Group|72063|5|Briefly described|p55|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen. Metamorphosed to amphibolite grade, broadly coeval with metamorphism of Stirling Range Formation (Dawson et al., 2003; Rasmussen et al., 2006), and granulite-amphibolite facies metamorphism in the Albany-Fraser Orogen (1215-1180 Ma) (Nelson et al., 1995; Spaggiari et al., 2014).||||||
27840|Mount Barren Group|72710|6|Mentioned|p4 Fig.2.|Paleoproterozoic|Paleoproterozoic|Shown as MBG on p4 Fig.2. Inferred to be part of Barren Basin.|1600 Ma to 1815 Ma.|||||
27840|Mount Barren Group|73084|6|Mentioned|p12|||Albany-Fraser Orogen, Northern Foreland.||||||
35605|Mount Belches Formation|23582|5|Briefly described|Map Legend|Archean|Archean|Includes the Santa Claus Member.||||||07-NOV-08
35605|Mount Belches Formation|23584|2|Defined|p4|Archean|Archean|Previously Mount Belches Beds. Age: c.2675 Ma. See also pages 8, 14. Geological Province: Yilgarn Craton. Max. thickness: 2500 m.||||||07-NOV-08
35605|Mount Belches Formation|60076|5|Briefly described|p14, p20|Archean|Archean|BIF-bearing sedimentary rocks.||||||07-NOV-08
35605|Mount Belches Formation|60555|5|Briefly described|p4 Tb. 1, p6 Fig. 3, p7, p10-12|Archean|Archean|Age of deposition: >2666+/-5Ma (Painter and Groenewald, 2001). Geological Province: Yilgarn Craton. Thick turbiditic rocks. See p11-12 for more detailed lithology.||||||07-NOV-08
35605|Mount Belches Formation|62093|5|Briefly described|p214 Fig. 1|Archean|Archean|Max. deposition age: 2666+/-5Ma (SHRIMP U-Pb). Geological Province: Yilgarn Craton. Mount is Mt in text of figure. See also p216 Tb. 1.||||||07-NOV-08
35605|Mount Belches Formation|64340|4|Described|p2 Fig. 1, p5 Fig. 3, p15, p18-19|Archean|Archean|Age: 2666+/-5Ma or c. 2667Ma.Geological Province:Yilgarn Craton. A sequence of thick metamorphosed turbiditic rocks. See p15 for more detailed info.||||||08-FEB-10
35605|Mount Belches Formation|64633|6|Mentioned|p39.|||Post-volcanic turbiditic basin, diagnostic of extensional rift settings.||||||
35605|Mount Belches Formation|64775|5|Briefly described|p8, 8-1, 11-1|||Thick sequence of metamorphosed, mainly clastic sedimentary rocks.||||Overlain by Penny Dam Conglomerate.||30-MAR-12
35605|Mount Belches Formation|65260|6|Mentioned|p6 Tb.1, p11|Neoarchean||Youngest deposition age 2665 Ma (zircons: Krapez et al. 2000).||||||
35605|Mount Belches Formation|65264|5|Briefly described|p20, p21, p50-51 Appdx. 1|Archean|Archean|Contains Santa Claus Member. Max. thickness: >2500m. Monotonous package of metamorphosed, multiply deformed wackes and mudstones. Detailed lithologies for several samples of this unit on p50-51 Appdx. 1.||||||07-FEB-11
35605|Mount Belches Formation|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton. Max depostional age: 2660+/-14 Ma.  See geochron file 177914.1.pdf, 177915.1.pdf (2007), 183145.1.pdf (2010).|||Includes Santa Claus Member and 7 unnamed subunits.|Intruded by Kiaki Monzogranite?|Varying proportions of wacke and mudstone, typically biotitic; rare banded iron-formation and pebbly sandstone beds; generally weakly metamorphosed but locally strongly hornfelsed; psammite; pelite.|06-AUG-15
35605|Mount Belches Formation|69181|6|Mentioned|p98|||Originally thought to be part of the Penny Dam Basin, but the discovery of two deformation fabrics has meant it likely belongs to older, late stage basins. ||||||
35605|Mount Belches Formation|70153|4|Described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Age derived from sample of metamorphosed volcaniclastic sandstone (177915.1.pdf) and constrains maximum depositional age of the sedimentary protolith.|2660 +/- 14 Ma (SHRIMP)||Includes Santa Claus Member.|Intruded and hornfelsed by Kiaki Monzongranite.|Interbanded psammite and pelite, hornfelsed and metasomatized wacke and mudstone. Biotite-quartz-feldspar pelite to para-amphibolite. Quartz psammite after wacke.|
35605|Mount Belches Formation|70802|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Sample GSWA 177915 (metasandstone) yielded a weighted mean 207Pb*/206Pb* date of 2660+\-14 Ma, interpreted as maximum depositional age of the metasandstone. Sample GSWA 177917 (metamorphosed tuffaceous sandstone) yielded a weighted mean 207Pb*/206Pb* date of 2667+\-5 Ma, interpreted as maximum depositional age of the tuffaceous sandstone. See 100k_geologyp10_lut.csv, 100k_geologysub10_lut.csv.|2660+\-14 Ma||Includes Santa Claus Member.|Intruded by, and underwent contact metamorphism by Kaiki Monzogranite.|Pelite, psammite, hornfelsed or metamsomatised wacke and mudstone, rare banded iron-formation and pebbly sandstone beds.|
35605|Mount Belches Formation|71168|5|Briefly described|p36||||||||Metamorphosed shale and chert.|
35605|Mount Belches Formation|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Metamorphosed to hornfel facies. Sample GSWA 177915 (metamorphosed volcaniclastic sandstone) yielded a weighted mean 207Pb/206Pb date of 2660+\-14 Ma, interpreted as maximum depositional age of the sandstone protolith. Sample GSWA 177917 (recrystallised, metamorphosed tufaceous sandstone) yielded a weighted mean 207Pb/206Pb date of 2667+\-5 Ma, interpreted as maximum depositional age of the sandstone protolith. Sample GSWA 183145 (metasandstone) yielded a weighted mean 207Pb/206Pb date of 2618+\-19 Ma, interpreted as maximum depositional age of the sandstone. See 100k_geologyp10_lut.csv, 100k_geologysub10_lut.csv.|2660+\-14 Ma||Includes Santa Clause Member.|Intruded by Kiaki Monzogranite.|Pelite and psammite; wacke and mudstone; hornselfed, metasomatised, rare BIFs and pebbly sandstone beds; weakly metamorphosed, locally strongly hornfelsed.|
35605|Mount Belches Formation|71493|6|Mentioned|p46|||Kurnalpi Terrane.|||||Includes metasandstone.|
35605|Mount Belches Formation|73238|5|Briefly described|p22-23, 27, 30|Archean|Archean|Kurnalpi Terrane. Is presented as Mt Belches Formation.|2666 +/- 5 Ma (MDA: Krapez et al., 2000).||||Includes a (folded) ferruginous chert horizon.|11-JAN-23
26047|Mount Bertram Sandstone|22496|6|Mentioned|p11||Neoproterozoic|Kuniandi Group||||||
26047|Mount Bertram Sandstone|23806|5|Briefly described|p1122|Paleoproterozoic|Paleoproterozoic|Of Kuniandi Group.||||||07-NOV-08
26047|Mount Bertram Sandstone|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26047|Mount Bertram Sandstone|32660|5|Briefly described|Table 6|||||||||
26047|Mount Bertram Sandstone|32728|6|Mentioned|Table 7|||See also Fig.16||||||
26047|Mount Bertram Sandstone|36551|6|Mentioned|Table 10|||||||||
26047|Mount Bertram Sandstone|36888|4|Described|p215|||||||||
26047|Mount Bertram Sandstone|36898|5|Briefly described|Table III|||||||||
26047|Mount Bertram Sandstone|37927|6|Mentioned|Fig.2|||||||||
26047|Mount Bertram Sandstone|38157|6|Mentioned|Table X|||||||||
26047|Mount Bertram Sandstone|44140|5|Briefly described|p301 fig 4-7|Neoproterozoic|Neoproterozoic|Of Mount Ramsay area. 120-180 m thick.||Kuniandi Group||Overlies Wirara Formation conformably. Is overlain unconformably by Egan Formation (Louisa Downs Group).|Micaceous and ferruginous sandstone; minor siltstone and shale, more frequent near base.|07-MAR-18
26047|Mount Bertram Sandstone|44231|5|Briefly described|Map Legend|Neoproterozoic III|Neoproterozoic III|Of the Kuniandi Group. Purple to grey, fine-grained micaceous and ferruginous sandstone, and purple fissile shale and siltstone. Age: c.610Ma. Geological Province: Louisa Basin. Mount is Mt in legend text.||||||26-MAY-05
26047|Mount Bertram Sandstone|44397|14|Not recorded|p.6,22, Table 3||Adelaidean|Kuniandi Group. Defn. on Tech.File E/52-9.||||||
26047|Mount Bertram Sandstone|44398|14|Not recorded|map legend||Adelaidean|||||||
26047|Mount Bertram Sandstone|45047|4|Described|p36|||||||||
26047|Mount Bertram Sandstone|48927|2|Defined|p15|Adelaidean|Adelaidean|||||||
26047|Mount Bertram Sandstone|63458|6|Mentioned|p873 Fig.2, p897 Fig.19. |Ediacaran|Ediacaran|||Unit in Kuniandi Group.||||
26047|Mount Bertram Sandstone|67484|6|Mentioned|p294 Tb.1|Ediacaran|Ediacaran|Mount Ramsay area, West Kimberley.  Mount is "Mt." in text.||Of the Kuniandi Group.||Underlain by the Wirara Formation. Is overlain by Louisa Downs Group.||
26047|Mount Bertram Sandstone|67620|5|Briefly described|p5|Ediacaran|Ediacaran|Mount Ramsay area, Kimberley region.||Kuniandi Group.||Overlies Wirara Formation. Is overlain by Egan Formation (Louisa Downs Group).||
26047|Mount Bertram Sandstone|68138|6|Mentioned|p156|Neoproterozoic|Neoproterozoic|Mount Ramsay area, Kimberley region.||Kuniandi Group.||||
26047|Mount Bertram Sandstone|68244|4|Described|p665|Neoproterozoic|Neoproterozoic|Louisa Basin, Kimberley region. Unlabelled on p660 Fig65.1.||Unit of Kuniandi Group.||Uppermost unit of the Mount Bertram Sandstone. Overlain by Egan Formation. Underlain by Wirara Formation.|Mauve quartzarenite.|
26047|Mount Bertram Sandstone|68473|6|Mentioned|p531|||Mount Ramsay.||Kuniandi Group||Equivalent to the Egan Formation.||
26047|Mount Bertram Sandstone|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Kuniandi Group.|||Purple to grey fine micaceous and ferruginous well sorted sandstone, and purple fissile shale and siltstone increasing towards the base; oscillation ripples, graded bedding, cross bedding, and clay pellet cavities|
68670|Mount Billroth Supersuite|63417|5|Briefly described|Map legend|Archean|Archean|Includes the Golden Eagle Orthogneiss. Age: 3199-3178Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
68670|Mount Billroth Supersuite|63441|4|Described|p35, p9 Tb. 2|Archean|Archean|Includes Flat Rocks Tonalite and Golden Eagle Orthogneiss. Age: 3200-3165Ma. Geological Province: Pilbara Craton (East Pilbara and Kurrana Terranes). See also p32 Fig. 11.||||||07-FEB-11
68670|Mount Billroth Supersuite|63538|6|Mentioned|p6 Fig. 3|Archean|Archean|Geological Province: Pilbara Craton.||||||19-APR-13
68670|Mount Billroth Supersuite|64654|5|Briefly described|Map Legend|Archaean|Archaean|Includes Golden Eagle Orthogeniss.  Age: 3199-3178Ma. Geological Province: Pilbara Craton.||||||
68670|Mount Billroth Supersuite|64656|5|Briefly described|Map Legend|Archaean|Archaean|Includes Golden Eagle Orthogneiss. Age: 3199-3178Ma. Geological Province: Kurrana Terrane (Pilbara Craton).||||||04-APR-13
68670|Mount Billroth Supersuite|65825|6|Mentioned|p32.|||Appendix 2 shows this as replacing the Kurrana Granitic Complex as the parent of Golden Eagle Orthogneiss, according to the GSWA databases.|||Includes Golden Eagle Orthogneiss.|||
68670|Mount Billroth Supersuite|66118|6|Mentioned|p147|||Pilbara Craton. East Pilbara Terrane.|In range of c. 3.2 Ga||||Granitic intrusions.|26-MAY-20
68670|Mount Billroth Supersuite|66217|5|Briefly described|p10, p38.|||East Pilbara Terrane. Granitic rocks. Emplaced possibly due to rifting during the Soanesville Event at 3200-3165 Ma.||||||
68670|Mount Billroth Supersuite|66302|6|Mentioned|p84|Mesoarchean|Mesoarchean||ca. 3200-3165 Ma||Includes the Flat Rocks Tonalite|||
68670|Mount Billroth Supersuite|67201|4|Described|p7 Fig.4, p19, p24, p26|Archean|Archean|Shown in Fig.4 as in West Pilbara Superterrane (xenocrystic zircon noted in Fig.4) and East Pilbara Terrane. In Kurrana Terrane. Age shown on p26 as 3180-3165 Ma.|3200-3165 Ma||Dalton Suite||Granitic intrusions. Gneissic metagranodiorite.|
68670|Mount Billroth Supersuite|68035|5|Briefly described|p289, 291, p286 Fig 3|Mesoarchean|Paleoarchean|Kurrana Terrane, SE Pilbara. Granitic rocks. Intruded rifted margin units (Soanesville Basin etc)|3200 - 3160 Ma|||||
68670|Mount Billroth Supersuite|68280|6|Mentioned|p3|Mesoarchean|Paleoarchean||3200-3160 Ma|||||
68670|Mount Billroth Supersuite|69167|6|Mentioned|geologyp_lut.csv|Mesoarchean|Mesoarchean||||Includes Golden Eagle Orthogneiss|||
68670|Mount Billroth Supersuite|69301|4|Described|p5 Fig.3, p12|||Pilbara Craton. West Pilbara Superterrane (xenocrystic zircon) and East Pilbara Terrane.|3.19-3.17 Ga||||Granitic rocks.|
68670|Mount Billroth Supersuite|69590|5|Briefly described|GEOL_LUT_CSV files|||Geological province: Pilbara Craton, West Australian Craton. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|||Includes Golden Eagle Gneiss.|||
68670|Mount Billroth Supersuite|69616|5|Briefly described|p162|Archean|Archean||c.3200-3165 Ma (Smithies et al., 2007).||Includes Dalton Suite.|||
68670|Mount Billroth Supersuite|70022|6|Mentioned|p115|||Pilbara Craton.||||||
68670|Mount Billroth Supersuite|70826|5|Briefly described|p8|Mesoarchean|Mesoarchean|East Pilbara Terrane.||||Intrudes the Soanesville Group.|Granites.|
68670|Mount Billroth Supersuite|70884|6|Mentioned|p122|Mesoarchean|Mesoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|c. 3.2-2.83 Ga|||||
68670|Mount Billroth Supersuite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, granodiorite|
68670|Mount Billroth Supersuite|72034|6|Mentioned|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Flat Rocks Tonalite, Golden Eagle Orthogneiss.|||
68670|Mount Billroth Supersuite|72251|5|Briefly described|p53-54|||Geological province: East Pilbara Terrane and West Pilbara Superterrane, Pilbara Craton. Locally intruded into the rifted margins of the East Pilbara Terrane, following rifting and breakup of the EPT at ~3.2 Ga.|||||Tonalite and granodiorite.|
68670|Mount Billroth Supersuite|72668|5|Briefly described|p4, p9-11, p14, p15, p16, p28|||West Pilbara Superterrane, Kurrana Terrane.  Dated samples include xenocrystic zircons from the Emu Pool Supersuite/Kelly Group and Callina Supersuite/Warrawoona Group, indicating derivation from recycling of mafic to felsic crust.|c. 3200-3170 Ma||Includes the Flat Rocks Tonalite and the Golden Eagle Orthogneiss.|||13-JAN-22
68670|Mount Billroth Supersuite|73598|6|Mentioned|p1212|Mesoarchean|Mesoarchean|East Pilbara Terrane.||||||
67853|Mount Boggola Formation|24544|4|Described|p47 Fig.35|Paleoproterozoic|Paleoproterozoic|Of Upper Wyloo Group. Volcanic rocks which divide the Ashburton Formation. Age: 1828+/-5 Ma. Geological Province: Ashburton Province.||||||07-NOV-08
67853|Mount Boggola Formation|63866|4|Described|p154|Orosirian|Orosirian|SHRIMP ages derived from Sircombe, 2003.|1829 +/- 5 Ma (SHRIMP U-Pb zircon)||||Felsic volcaniclastic rock.|
35643|Mount Boreas Adamellite|23281|5|Briefly described|p7||Siderian|Max Age: 2480 (+/-) 30 Ma (Roddick and Libby, 1995).||||||
39759|Mount Cassiterite Pegmatite Group|24193|5|Briefly described|p886 Tb.5|Archean|Archean|Mount is Mt. in text. Geological Province: Pilbara Craton.||||||07-NOV-08
41460|Mount Christine Granite|50437|5|Briefly described|p4.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Kevins Dam Suite (Sally Downs Supersuite). Age: 1808-1819 +/- 4Ma (SHRIMP). Used interchangeably with Mount Christine Granitoid.||||||31-JAN-14
41460|Mount Christine Granite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Data from OZCHRON1. Comment: (1808 Ma) 'An igneous crystallisation age for the unfoliated granite at Crocodile Pool. (1817 Ma) 'This is the igneous crystallisation age of this deformed (early) phase'.|cryst age 1808+/-3 Ma, 1817+/-4 Ma U/Pb SHRIMP|Kevins Dam Suite|||Coarsely porphyritic, medium-grained biotite monzogranite.|03-AUG-15
41460|Mount Christine Granite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv.|1808-1817 Ma|Kevins Dam Suite|||Coarsely porphyritic, medium grained biotite monzogranite.|
41460|Mount Christine Granite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2.|1808-1808 Ma (Isotopic)|Unit of Kevins Dam Suite.|||Coarsely porphyritic, medium-grained biotite monzogranite|
41460|Mount Christine Granite|70154|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1808 Ma|Kevins Dam Suite|||Coarsely porphyritic, medium-grained biotite monzogranite|
41460|Mount Christine Granite|71267|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma).|1808+\-3 Ma (isotopic)|Unit of Kevins Dam Suite.|||Medium- to coarse-grained biotite monzogranite and hornblende-biotite monzogranite and granodiorite.|
41460|Mount Christine Granite|71397|5|Briefly described|p8|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen. |1808+\-3 Ma|||Intrudes into Olympio Formation.||
79016|Mount Clifford Komatiite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2720 - 2680 Ma (inferred).|Marshall Pool Subgroup|||Komatiitic basalt; relict pyroxene-spinifex texture; metamorphosed. Talc-serpentine-chlorite schist, komatiite; locally preserved relict olivine spinifex texture; metamorphosed. Peridotite, commonly serpentinized; metamorphosed.|
79016|Mount Clifford Komatiite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2726-2680 Ma (inferred)|Unit of Marshall Pool Subgroup.||Underlain by Hangover Formation. Overlain by Mount Fouracre Basalt.|Komatiitic basalt; relict pyroxene-spinifex texture; metamorphosed; talc-chlorite-carbonate schist; peridotite; relict olivine-cumulate texture, commonly serpentinized; metamorphosed.|
79016|Mount Clifford Komatiite|73596|6|Mentioned|p1159, 1162-1163|||Leonora eastern domain, Kalgoorlie Terrane. Described as ""affiliated"" with the Two Sisters Subgroup based on shared lithostatigraphic, geochemical and textural properties. Appears as Mt Clifford Formation on p1162.||Marshall Pool Subgroup.||Overlies Hangover Basalt. Is overlain by Mount Fouracre Basalt.||
23815|Mount Close Chert Member|14019|5|Briefly described|p20|||Of the Antrim Plateau Volcanics.  Contains conical stromatolites.  Probably Neoproterozoic in age?||||||
23815|Mount Close Chert Member|23216|6|Mentioned|p36|||||||||
23815|Mount Close Chert Member|23328|5|Briefly described|1031 Fig.2|Early Cambrian|Early Cambrian|||||||07-SEP-09
23815|Mount Close Chert Member|23621|6|Mentioned|p35|||||||||
23815|Mount Close Chert Member|40993|6|Mentioned|Fig.1|||||||||
23815|Mount Close Chert Member|41840|4|Described|p40|||||||||
23815|Mount Close Chert Member|41864|4|Described|p10|||||||||
23815|Mount Close Chert Member|41866|5|Briefly described|Map legend|Early Cambrian||||||||
23815|Mount Close Chert Member|44230|5|Briefly described|Map Legend||Early Cambrian|In Ord and Bonaparte Basins.||||||
23815|Mount Close Chert Member|44868|5|Briefly described|Map Legend|Boomerangian|Ordian|||||||
23815|Mount Close Chert Member|65337|6|Mentioned|p94.|||||Unit in Antrim Plateau Volcanics.||||
23815|Mount Close Chert Member|67860|4|Described|p420 Tb. 4-18, p421 fig 4-86|Early Cambrian|Early Cambrian|Hot springs deposits. 0-5 m thick. Type section details given. Contains stromatolites.||Antrim Plateau Volcanics|||Chert; intraformational breccia.|
23815|Mount Close Chert Member|69445|5|Briefly described|p30:3-4, 17|Early Cambrian|Early Cambrian|Mory and Beere (1985). Recognised in DIXON RANGE and LISSADELL map areas, with an equivalent in NT. Also abbreviated to Mount Close Member on p30:3-4.||Antrim Plateau Volcanics.|||Stromatolitic limestone and matrix-supported basalt breccia, silicified at the surface.|12-JUL-16
23815|Mount Close Chert Member|70315|6|Mentioned|p23|||Kalkarindji Province. 5m thick.||Antrim Plateau Volcanics||Overlies the Malley Springs Sandstone Member. Overlain by the Bingy Bingy Basalt Member.||
27842|Mount Disaster Porphyry|23722|4|Described|p10|Proterozoic|Proterozoic|Intrudes Whitewater Volcanics.   Geological Province: Hooper Complex||||||
27842|Mount Disaster Porphyry|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1860Ma. Geological province: Kimberley Province (West).||||||07-FEB-11
27842|Mount Disaster Porphyry|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
27842|Mount Disaster Porphyry|30525|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27842|Mount Disaster Porphyry|30533|4|Described|p13|||On Table 1||||||
27842|Mount Disaster Porphyry|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27842|Mount Disaster Porphyry|30896|4|Described|p13|||Lower Proterozoic||||||
27842|Mount Disaster Porphyry|30897|4|Described|p9|||||||||
27842|Mount Disaster Porphyry|30898|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27842|Mount Disaster Porphyry|31226|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27842|Mount Disaster Porphyry|32728|6|Mentioned|Fig.3|||||||||
27842|Mount Disaster Porphyry|36885|4|Described|p171|||||||||
27842|Mount Disaster Porphyry|37462|6|Mentioned|Fig.4.6|||||||||
27842|Mount Disaster Porphyry|41987|5|Briefly described|p73|||||||||
27842|Mount Disaster Porphyry|42710|5|Briefly described|map legend|Proterozoic||||||||
27842|Mount Disaster Porphyry|42811|5|Briefly described|p10|||||||||
27842|Mount Disaster Porphyry|42814|5|Briefly described|p7|||||||||
27842|Mount Disaster Porphyry|42815|5|Briefly described|map|||||||||
27842|Mount Disaster Porphyry|43281|5|Briefly described|Map legend||Proterozoic|||||||
27842|Mount Disaster Porphyry|44155|4|Described|p234 Tb.3-2, p241 Tb.3-4 |Paleoproterozoic|Paleoproterozoic|Comagmatic with Whitewater Volcanics; Bickleys and Castlereagh Hill Porphyries.||Hooper Complex||Intruded by Mondooma Granite. Intrudes or unconformably overlies Halls Creek Group.|Grey to pale pink porphyritic biotite microgranite; phenocrysts of quartz, K-feldspar (2-5cm) and plagioclase.|
27842|Mount Disaster Porphyry|48931|3|Fully described|p22|||||||||
27842|Mount Disaster Porphyry|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite.||||||07-NOV-08
27842|Mount Disaster Porphyry|68078|6|Mentioned|p14 figure 10|Paleoproterozoic|Paleoproterozoic|||Paperbark Supersuite||||
27842|Mount Disaster Porphyry|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Paperbark Supersuite|||Foliated, porphyritic, biotite metamicromonzogranite; phenocrysts of K-feldspar, plagioclase, and quartz.|03-AUG-15
27842|Mount Disaster Porphyry|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone. See 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|1864-1852 Ma (inferred)|Unit of Paperbark Supersuite.|||Foliated, porphyritic, biotite metamicromonzogranite; phenocrysts of K-feldspar, plagioclase, and quartz|
27842|Mount Disaster Porphyry|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Kimberley Craton.||Unit in Paperbark Supersuite.|||Foliated, porphyritic, biotite metamicromonzogranite; phenocrysts of K-feldspar, plagioclase and quartz.|
27842|Mount Disaster Porphyry|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province; Halls Creek Orogen; North Australian Craton.||Paperbark Supersuite.|||Foliated, porphyritic, biotite metamicromonzogranite; phenocrysts of K-feldspar, plagioclase and quartz.|
27842|Mount Disaster Porphyry|70154|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic||1852-1864 Ma|Paperbark Supersuite|||Foliated, porphyritic, biotite metamicromonzogranite; phenocrysts of K-feldspar, plagioclase, and quartz.|
27842|Mount Disaster Porphyry|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (183 -1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyp_lut.csv, 1m_interpgeop_lut.csv.|1864-1852 Ma (inferred)|Unit of Paperbark Supersuite.|||Foliated, porphyritic, biotite metamicromonzogranite; phenocrysts of K-feldspar, plagioclase, and quartz|
27842|Mount Disaster Porphyry|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen, North Australian Craton.||Paperbark Supersuite.|||Foliated, porphyritic, biotite metamicromonzogranite; phenocrysts of K-feldspar, plagioclase and quartz.|
27842|Mount Disaster Porphyry|72437|5|Briefly described|p34-37|||Whole-rock analyses are provided.|||||Porphyry.|
22413|Mount Ellis Gabbro|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).  See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2702-2692 Ma (inferred)||||Quartz-bearing gabbro locally grading into granophyre; metamorphosed; minor to locally dominant leucogabbro; pyroxenite, metamorphosed.|
22415|Mount Fairbairn Monzogranite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  Age: c. 1835-1805 Ma.||||||07-NOV-08
22415|Mount Fairbairn Monzogranite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs Supersuite. Age: 1825Ma. Geological province: Kimberley Province.||||||07-FEB-11
22415|Mount Fairbairn Monzogranite|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite. Coarse- to fine-grained, locally porphyritic, partly recrystallised biotite monzogranite; associated with gabbro; rich in mafic inclusiones locally.||||||07-NOV-08
22415|Mount Fairbairn Monzogranite|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Sally Downs Supersuite. Used interchangeably with Mount Fairbairn Granite.||||||07-NOV-08
22415|Mount Fairbairn Monzogranite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Sally Downs Supersuite.|||Coarse to fine grained locally porphyritic partly recrystallised biotite monzogranite; associated with gabbro and locally rich in mafic inclusions|
28200|Mount Forster Sandstone|22496|4|Described|p11||Neoproterozoic|Of the Albert Edward Group.   Overlain by the Elivire Formation.  Geological Province:  Wolfe Basin||||||16-AUG-04
28200|Mount Forster Sandstone|22547|4|Described|p28||Neoproterozoic III|Of the Albert Edward Group. Geological province: Wolfe Creek Basin. Thickness: 40 m. Overlies Ranford Formation, overlain by Antrim Plateau Volcanics||||||14-NOV-06
28200|Mount Forster Sandstone|22777|5|Briefly described|Map|||Albert Edward Group, Wolfe Basin||||||
28200|Mount Forster Sandstone|23621|4|Described|p34|Neoproterozoic|Neoproterozoic|See also page 9 table 1. Of Albert Edward Group. Overlying unit Elvire Formation. Underlying unit Ranford Formation. Wolfe Basin. Max. thickness: 150 m.||||||
28200|Mount Forster Sandstone|23622|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Albert Edward Group. Geological Province: Wolfe Basin.||||||
28200|Mount Forster Sandstone|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|Of Albert Edward Group.||||||
28200|Mount Forster Sandstone|24173|4|Described|p25, p11 Tb.2|Neoproterozoic III|Neoproterozoic III|Of the Albert Edward Group.  Whitish, quartz sandstone to slightly lithic sandstone. Overlain by Elvire Formation. Geological Province: Wolfe Basin. Max Thickness: 150m.||||||06-APR-05
28200|Mount Forster Sandstone|29813|4|Described|Table 2|||||||||
28200|Mount Forster Sandstone|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
28200|Mount Forster Sandstone|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
28200|Mount Forster Sandstone|32660|5|Briefly described|Table 6|||||||||
28200|Mount Forster Sandstone|32728|5|Briefly described|Table 6|||||||||
28200|Mount Forster Sandstone|36532|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
28200|Mount Forster Sandstone|36551|6|Mentioned|Table 12|||||||||
28200|Mount Forster Sandstone|36888|4|Described|p214|||||||||
28200|Mount Forster Sandstone|36898|5|Briefly described|Table II|||||||||
28200|Mount Forster Sandstone|37927|6|Mentioned|Fig.2|||||||||
28200|Mount Forster Sandstone|38157|6|Mentioned|Table X|||||||||
28200|Mount Forster Sandstone|41429|6|Mentioned|p247|||||||||
28200|Mount Forster Sandstone|43299|5|Briefly described|Map Legend||Neoproterozoic|of Albert Edward Group.||||||
28200|Mount Forster Sandstone|43303|5|Briefly described|Map Legend||Neoproterozoic|of Albert Edward Group.||||||
28200|Mount Forster Sandstone|43853|5|Briefly described|Map Legend||Proterozoic|||||||
28200|Mount Forster Sandstone|43855|5|Briefly described|Map Legend||Proterozoic|||||||
28200|Mount Forster Sandstone|44140|5|Briefly described|p301 fig 4-7, p302 Tb.4-2|Neoproterozoic|Neoproterozoic|Osmond Range (East Kimberley) area. 94 m thick; glacials apparently missing at base of Group.||Albert Edward Group||Unconformably overlies Duerdin Group. Overlain by Elvire Formation conformably.|Quartz sandstone; minor shale and siltstone.|07-MAR-18
28200|Mount Forster Sandstone|44230|5|Briefly described|Map Legend||Proterozoic|||||||
28200|Mount Forster Sandstone|44317|4|Described|Table 3, p.7||Adelaidean|||||||
28200|Mount Forster Sandstone|44318|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
28200|Mount Forster Sandstone|44324|14|Not recorded|p.10||Adelaidean|Tb.2 (Adelaidean) of Albert Edward Group.||||||
28200|Mount Forster Sandstone|44325|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
28200|Mount Forster Sandstone|44363|5|Briefly described|p.6,14||Adelaidean|(in Albert Edward Group).||||||
28200|Mount Forster Sandstone|44364|14|Not recorded|map legend|||||||||
28200|Mount Forster Sandstone|44868|5|Briefly described|Map Legend||Phanerozoic|||||||
28200|Mount Forster Sandstone|45047|2|Defined|p94|Adelaidean|Adelaidean|See also p36.||||||18-MAY-15
28200|Mount Forster Sandstone|45140|2|Defined|p13, p59, Appx.p36|||Dow and Gemuts (1969). Named after Mount Forster. Unnamed basin NW of Birrindudu Basin. Type section is Brim Creek in Albert Edward Range, at 18deg 15'S, 128deg 00'E, in the Gordon Downs sheet area. Forms prominent strike ridges and cuestas. 200m thick.||Basal Albert Edward Group.||Unconformably overlies Ranford Formation. Is overlain conformably by Elvire Formation.|Quartz arenite, sublithic arenite and minor conglomerate.|
28200|Mount Forster Sandstone|48927|6|Mentioned|Table 1|||Refers Dow & Gemuts (1969)||||||
28200|Mount Forster Sandstone|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Albert Edward Group. Geological Province: Wolfe Creek Basin. Fine to medium grained quartz sandstone; minor pebbly sandstone and conglomerate.||||||
28200|Mount Forster Sandstone|63458|6|Mentioned|p873 Fig.2, p897 Fig.19. |Ediacaran|Ediacaran|||Unit in Albert Edward Group.||||
28200|Mount Forster Sandstone|64104|6|Mentioned|p62 fig.1, p71 Tb. 2, p72 Fig.8|Neoproterozoic|Neoproterozoic|||Unit in Albert Edward Group.||Is overlain by Elvire Formation.||
28200|Mount Forster Sandstone|67484|6|Mentioned|p294, p295 Fig.2|Ediacaran|Ediacaran|East Kimberley. Mis-spelt as Foster on p294.||Of the Albert Edward Group.||Overlain by the Elvire Formation. Underlain by the Ranford Formation.||
28200|Mount Forster Sandstone|67620|5|Briefly described|p5|Ediacaran|Ediacaran|East Kimberley region.||Albert Edward Group.||Overlies Ranford Formation (Duerdin Group). Is overlain by Elvire Formation.||
28200|Mount Forster Sandstone|68138|6|Mentioned|p153, 156|Neoproterozoic|Neoproterozoic|East Kimberley region. Appears as Mount Foster Sandstone on p153.||Albert Edward Group.||||
28200|Mount Forster Sandstone|68244|4|Described|p660,667|Neoproterozoic|Neoproterozoic|East Kimberly area, Kimberley region. Glaciogenic unit deposited during of Egan Glaciation.||Unit of Albert Edward Group.||Lowermost unit of Albert Edward Group. Overlain by Elvire Formation.||
28200|Mount Forster Sandstone|68473|6|Mentioned|p531|||||||||
28200|Mount Forster Sandstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Wolfe Creek Basin||Of Albert Edward Group.|||Fine- to medium-grained quartz sandstone; minor pebbly sandstone and conglomerate.|03-AUG-15
28200|Mount Forster Sandstone|69165|5|Briefly described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|See also 100k_xsecgeop_lut.csv. ||Albert Edward Group|||Fine to medium grained quartz sandstone; minor pebbly sandstone and conglomerate.|
28200|Mount Forster Sandstone|69437|6|Mentioned|p22:4-5|||Wolfe Basin. May be equivalent to Kinevans Sandstone.||Albert Edward Group.||||12-JUL-16
28200|Mount Forster Sandstone|69442|6|Mentioned|p27:6|||||Albert Edward Group.||Possibly equivalent to the Kinevans Sandstone.||12-JUL-16
28200|Mount Forster Sandstone|69445|5|Briefly described|p30:16-17|||Purnululu National Park.||Albert Edward Group.||Is overlain unconformably by Antrim Plateau Volcanics.||12-JUL-16
28200|Mount Forster Sandstone|69634|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1.|635-541 Ma (Inferred)|Unit of Albert Edward Group.|||Fine- to medium-grained quartz sandstone; minor pebbly sandstone and conglomerate|
28200|Mount Forster Sandstone|70154|6|Mentioned|100k_interpgeop_lut.csv|Fortunian|Ediacaran||541-635 Ma|Albert Edward Group||||
28200|Mount Forster Sandstone|71267|4|Described|GEOL_LUT_CSV files|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|635-541 Ma (inferred)|Unit of Albert Edward Group.|||Cross-bedded, mainly medium grained sublithic and quartz sandstone with minor shale and siltstone, and iron-stained pebbly sublithic sandstone and conglomerate near base|
28200|Mount Forster Sandstone|73255|6|Mentioned|p534 Fig.2|Ediacaran|Ediacaran|Written as Mt Forster Sandstone in text.||Albert Edward Group||Disconformably overlies the Ranford Formation, underlies the Elvire Formation.||
79019|Mount Fouracre Basalt|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2720 - 2680 Ma (inferred).|Marshall Pool Subgroup|||Mafic schist derived from basalt, amygdaloidal basalt, aphyric basalt, basalt, komatiitic basalt; metamorphosed.|
79019|Mount Fouracre Basalt|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2726-2680 Ma (inferred)|Unit of Marshall Pool Subgroup.||Underlain by Mount Clifford Komatiite.|Basalt; amygdaloidal, aphyric, metamorphosed; komatiitic basalt; relict pyroxene-spinifex texture; metamorphosed; mafic schist derived from basalt.|
79019|Mount Fouracre Basalt|73596|6|Mentioned|p1159, 1162-1163|||Leonora eastern domain, Kalgoorlie Terrane. Described as ""affiliated"" with the Two Sisters Subgroup based on shared lithostatigraphic, geochemical and textural properties.||Marshall Pool Subgroup.||Overlies Mount Clifford Formation. Is overlain by Gindalbie Group.||
78982|Mount Gibson Formation|68698|5|Briefly described|p4|Mesoarchean|Mesoarchean|Felsic volcanic and volcaniclastic rocks.||Golden Grove Group.||||
78982|Mount Gibson Formation|70796|6|Mentioned|155879.1.pdf.|||Murchison Domain.||||Coeval with the Thundelarra Supersuite.|Felsic metavolcanic rock.|
78982|Mount Gibson Formation|70830|5|Briefly described|p7, p9|Mesoarchean|Mesoarchean|Ages are derived from Yeats et al, 1996 and Wang et al, 1998.|c. 2935 Ma|Murchison Supergroup|||Volcano-sedimentary rocks.|
78982|Mount Gibson Formation|71269|5|Briefly described|geochron files|||||||Coeval with Thunderlarra Supersuite/Bunnawarra Suite.||
78787|Mount Gibson Iron Formation|63153|6|Mentioned|p1367|||Of Lascelles (2006). Shows massive carbonate replacement of chert.||||||14-MAR-14
70608|Mount Glasse formation|61898|5|Briefly described|p109 Fig. 1|||Informal name.||||||
35641|Mount Goode Basalt|7471|6|Mentioned|p20.|||Kathleen Valley area, Agnew-Wiluna belt. Minor Cu mineralisation in pyrite-chalcopyrite-quartz veins, commonly with Au and Ag, is found in mafic hosts spatially related to NNW-trending shear zones in this unit.||||||
35641|Mount Goode Basalt|23281|6|Mentioned|p5|||||||||
35641|Mount Goode Basalt|23595|5|Briefly described|p7|||Underlain by Kathleen Valley Gabbro. Geological Province: Yilgarn Craton.||||||30-SEP-08
35641|Mount Goode Basalt|23611|5|Briefly described|p17|Archean|Archean|See also page 30 Appendix 1. Geological Province: Yilgarn Craton.||||||07-NOV-08
35641|Mount Goode Basalt|24135|5|Briefly described|p12|||||||||
35641|Mount Goode Basalt|24174|5|Briefly described|p4, p6, p31, p34|Archean|Archean|Geological Province: Eastern Goldfields.||||||07-NOV-08
35641|Mount Goode Basalt|43288|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
35641|Mount Goode Basalt|64586|5|Briefly described|Map legend|Archean|Archean|Metamorphosed tholeiitic basalt and metamorphosed plagio-phyric tholeiitic basalt.||||||23-DEC-09
35641|Mount Goode Basalt|65264|5|Briefly described|p18, p32|||Includes an extensive suite of massive, fine-grained tholeiitic metabasalt in the Agnew-Wiluna greenstone belt; commonly porphyritic.||||||07-FEB-11
35641|Mount Goode Basalt|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Mesoarchean|Eastern Goldfields Superterrane, Yilgarn Craton|||Includes unnamed subunit.||Tholeiitic basalt; metamorphosed; plagioclase-phyric tholeiitic basalt; phenocrysts up to 20 cm long; metamorphosed.|06-AUG-15
35641|Mount Goode Basalt|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Tholeiitic basalt. Plagioclase-phyric tholeiitic basalt with phenocrysts up to 20 cm long. Metamorphosed.|
35641|Mount Goode Basalt|71270|4|Described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton.|||||Tholeiitic and plagioclase-phyric tholeiitic basalt; phenocrysts up to 20 cm long; metamorphosed|
35641|Mount Goode Basalt|73596|6|Mentioned|p1152, 1155-1157, 1169|||Kathleen Valley Domain, Agnew-Wiluna Greenstone Belt. Over 1000m thick. Layering is consistently overturned; younging towards SE or ESE.||||Is structurally overlain by Cosmos Volcanic Complex. Is intruded by Kathleen Valley Layered Igneous Complex.|Sequence of pillow-textured to massive, tholeiitic, locally feldspar-porphyritic to megacrystic basalts.|
75073|Mount Goodwin Subgroup|69452|4|Described|p36:8, 15, 19-21|||Helby (1974); redefined in Gorter et al. (2009). Petrel Sub-basin, Bonaparte Basin. Extensive in the subsurface; represented onshore by a thin 20m-thick succession near Port Keats. Up to 670m thick.||Kinmore Group.|Ascalon, Mairmull, Penguin, Fishburn Formations.|Unconformably overlies Hyland Bay Subgroup. Is overlain unconformably by Sahul Group.|Shale, claystone, siltstone and minor sandstone.|12-JUL-16
75073|Mount Goodwin Subgroup|69454|5|Briefly described|p38:4|Olenekian|Changhsingian|Petrel Sub-basin, Bonaparte Basin.||Kinmore Group.|Penguin, Mairmull, Ascalon, Fishburn Formations.|Overlies Hyland Bay Subgroup. Is overlain by Troughton Group.||12-JUL-16
75073|Mount Goodwin Subgroup|69673|5|Briefly described|p153 fig 125, p173|||570-670m thick.||Kinmore Group|Includes Penguin Formation, Mairmull Formation, Ascalon Formation, Fishburn Formation|Unconformably overlain by Troughton Group|Siltstone and shale.|
75073|Mount Goodwin Subgroup|70061|5|Briefly described|Petrel Sub-basin Figs.2 & 3, p2-3|Middle Triassic|Early Triassic|See also Regional geology: Figs.6-8, p10-12. Vulcan: Fig.2. Marine shales form a regional seal for Permian reservoirs, eg the Hyland Bay Subgroup. Appears as Mount Goodwin Formation on p12.||Kinmore Group.|Penguin, Mairmull, Ascalon and Fishburn Formations.|Overlies Hyland Bay Subgroup. Is overlain by Cape Londonderry Formation.|Includes transgressive, thick marine shales.|12-JUL-16
75073|Mount Goodwin Subgroup|71146|5|Briefly described|p6|Lopingian|Lopingian|Bonaparte Basin.||||Overlies the Hyland Bay Subgroup. Overlain by the Osprey Formation.|Mudstone.|
68506|Mount Gregory Monzodiorite|63441|2|Defined|p10 Tb. 2, p36|Archean|Archean|Of the Orpheus Supersuite - within the structure of Harding Granitic Complex. Age: 3016+/-14Ma. Geological province: Pilbara Craton. Intrudes Andover Intrusion which is genetically related. See also p37.||||||07-FEB-11
68506|Mount Gregory Monzodiorite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Orpheus Supersuite. Geological province: Pilbara Craton. Massive, medium- to coarse-grained monzodiorite; metamorphosed.||||||07-NOV-08
68506|Mount Gregory Monzodiorite|64580|4|Described|map legend||Mesoarchean|Of Orpheus Supersuite. Massive, medium- to coarse-grained monzodiorite; metamorphosed.||||||15-DEC-08
68506|Mount Gregory Monzodiorite|67201|4|Described|p16-17 Fig.9|Archean|Archean|Pilbara Craton. In Roebourne-Karratha area.||Orpheus Supersuite|||Massive, medium- to coarse-grained monzodiorite; metamorphosed.|
68506|Mount Gregory Monzodiorite|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Orpheus Supersuite.|||Massive, medium- to coarse-grained monzodiorite; metamorphosed|
68506|Mount Gregory Monzodiorite|70775|5|Briefly described|p15, p46, p49|||Pilbara Craton.|3016 +/- 4 Ma (Nelson 2001j)|Orpheus Supersuite|||Massive, medium- to coarse-grained monzodiorite; metamorphosed.|
68506|Mount Gregory Monzodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzodiorite|
68506|Mount Gregory Monzodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|De Grey Superbasin.|3016+/-4 Ma.|Orpheus Supersuite|||Monzodiorite; massive, medium- to coarse-grained; metamorphosed.|
28798|Mount Gytha Lamproite|41158|5|Briefly described|Table 43|||||||||
77867|Mount Herbert Gabbro|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2696 Ma (inferred).|Leviathan Suite|||Gabbro; metamorphosed.|
77867|Mount Herbert Gabbro|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2696 Ma (inferred)|Unit of Leviathan Suite.|||Gabbro, metamorphosed.|
74896|Mount Holmes Gabbro|69152|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|||Giles Suite|Informally divided in to two unnamed subunits.||Dolerite; gabbro sill with minor dolerite.|06-AUG-15
74896|Mount Holmes Gabbro|69583|5|Briefly described|p59, p109; Plate 2|Proterozoic|Proterozoic|Crops out near Sandstone. Typically shallow-dipping. Extends over 200km east from the Windimurra Igneous Complex to the Eastern Goldfields Superterrane. SHRIMP U-Pb baddeleyite crystallisation age.|c.1070 Ma (Wingate et al., 2008).|Warakurna Supersuite.|||Gabbro sill.|
74896|Mount Holmes Gabbro|70153|5|Briefly described|100k_geologyp10_lut.csv|Mesoproterozoic|Mesoproterozoic|See also 500k_interpgeop14_lut.csv.|1070 +/- 18 Ma (isotopic).|Giles Suite|||Gabbro sill and dolerite; metamorphosed.|
74896|Mount Holmes Gabbro|70419|5|Briefly described|p15, p19|Proterozoic|Proterozoic|A sill of this unit produces a highly reflective unit in seismic line 10GA-YU2.||||Correlates with Warakurna Supersuite.|Gabbro sill.|
74896|Mount Holmes Gabbro|70830|5|Briefly described|p23, p25|Stenian|Stenian|Youanmi Terrane. Age is a SHRIMP U-Pb baddeleyite date. In places 5m thick. Forms a prominent feature on aeromagnetic images and appears to extend for more than 400km.|c. 1070 Ma (Wingate et al, 2008)||||Medium- to coarse-grained gabbro.|
74896|Mount Holmes Gabbro|71270|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Of Warakurna Large igneous Province. Events: Alice Springs Orogeny (450 - 295 Ma); Petermann Orogeny (580 - 520 Ma); Paterson Orogeny (635 - 540 Ma); Warakurna Supersuite Magmatic Event (1084 - 1040 Ma); Giles Event (1085 - 1040 Ma).|1070+\-18 Ma|Unit of Giles Suite.|||Dolerite and gabbro sill.|
74896|Mount Holmes Gabbro|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic||1070+/-18 Ma|Warakurna Supersuite|||Gabbro; metamorphosed.|
28800|Mount Hunt Sill|22596|6|Mentioned|Table 1 p409|Archean|Archean|Spelt Mt Hunt Sill. See also Fig.5 p416||||||07-NOV-08
28800|Mount Hunt Sill|41249|6|Mentioned|p20|||||||||
28800|Mount Hunt Sill|43102|5|Briefly described|Fig.2|||actually spelt Mt Hunt Sill||||||
28800|Mount Hunt Sill|43496|6|Mentioned|9|||||||||
75712|Mount James Subgroup|65545|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Pooranoo Metamorphics, Gascoyne Province. Includes Spring Camp Formation.  c. 1680 Ma.||||||
75712|Mount James Subgroup|65549|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Pooranoo Metamorphics. Includes Spring Camp Formation. Overlies Camel Hills Metamorphics, underlies Yilgatherra Formation, Edmund Group.||||||
75712|Mount James Subgroup|66110|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Shown as comprising the same units as the Pooranoo Metamorphics. These include Biddenew and Spring Camp Formations, as well as three unnamed units of metamorphosed shale, sandstone and conglomerate, and schists.||||||
75712|Mount James Subgroup|66299|4|Described|p4 Fig.2, p22, pp215-220.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Subdivision into its two Formations was conducted during the second edition mapping of the type area on southern PINK HILLS and YINNETHARRA in 2007-08 (Sheppard et al. 2008; Johnson et al. 2010). At least 700m thick.|Deposited after c.1760 Ma and before c.1680 Ma.|Basal unit in Pooranoo Metamorphics.|Includes Biddenew Formation and Spring Camp Formation.|Unconformably overlies Mumba Psammite, Halfway Gneiss and Moorarie Supersuite granites. Intruded by granite and pegmatite of Thirty Three Supersuite.|Pelitic and psammitic schists, metamorphosed quartz sandstone, feldspathic metasandstone and metaconglomerate.|
75712|Mount James Subgroup|66579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.||Shown as the only unit in Pooranoo Metamorphics.|Includes Biddenew and Spring Camp Formations, as well as two mapped but unnamed units: one phyllite and slate, the other cobble and boulder metaconglomerate.||Quartzose schist; quartzose and feldspathic metasandstones; phyllite, slate, metaconglomerate.|
75712|Mount James Subgroup|66950|5|Briefly described|p12|Statherian|Statherian|Mount James Subgroup written as Mt in text. Formerly the Mount James Formation (Hunter 1990).||Of the Pooranoo Metamorphics.|Includes Spring Camp Formation and Biddenew Formation.||Comprises metamorphosed fluvial conglomerates and sandstones, and shallow-marine sandstones.|16-DEC-16
75712|Mount James Subgroup|67247|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.||Unit in Pooranoo Metamorphics.|Includes Spring Camp Formation.|||
75712|Mount James Subgroup|67371|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.||Unit in Pooranoo Metamorphics.|Includes Biddenew and Spring Camp Formations.|||
75712|Mount James Subgroup|67373|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.||Unit in Pooranoo Metamorphics.|Includes Biddenew Formation.|||
75712|Mount James Subgroup|67843|5|Briefly described|p1. |||Gascoyne Province.||Unit in Pooranoo Metamorphics.||||
75712|Mount James Subgroup|68521|5|Briefly described|Map Legend|Statherian|Statherian||c.1780-1680 Ma|Of the Pooranoo Metamorphics.|Includes Spring Camp Formation and Biddenew Formation.|||
75712|Mount James Subgroup|68522|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. ||Of the Pooranoo Metamorphics.|Includes Spring Camp Formation and Biddenew Formation.|||
75712|Mount James Subgroup|69003|5|Briefly described|p33|Paleoproterozoic|Paleoproterozoic|Gascoyne Province, Capricorn Orogen. Up to 700m thick.||Pooranoo Metamorphics.|Coor-de-wandy Formation||A series of poorly sorted, immature, fluvial sandstones, pebbly sandstones, and conglomerates that are overlain by locally mature, well-sorted, shallow-marine quartz sandstones.|
75712|Mount James Subgroup|69028|5|Briefly described|Map Legend|Statherian|Statherian|Gascoyne Province.||Of the Pooranoo Metamorphics.|||Pelitic and psammitic schist, metamorphosed quartz sandstone, feldspathic metasandstone, and metaconglomerate.|06-MAY-14
75712|Mount James Subgroup|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|||Pooranoo Metamorphics|Includes Biddenew Formation, Spring Camp Formation, Mount James Formation||Pelitic and psammitic schist, metamorphosed quartz sandstone, feldspathic metasandstone and metaconglomerate.|
75712|Mount James Subgroup|69583|5|Briefly described|p130, Plate 3.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Age range from parent.|1758-1683 Ma.|Pooranoo Metamorphics.|||Pelitic and psammitic schist, metamorphosed quartz sandstone, feldspathic metasandstone and metaconglomerate.|
75712|Mount James Subgroup|70795|6|Mentioned|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|West Australian Craton|1758-1683 Ma|Pooranoo Metamorphics|Includes Biddenew Formation, Spring Camp Formation|||
75712|Mount James Subgroup|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Gascoyne Province, Capricorn Orogen.|Max age 1758+/-18 Ma, min ~1682 Ma.|Pooranoo Metamorphics|||Pelitic and psammitic schist, metamorphosed quartz sandstone, feldspathic metasandstone and metaconglomerate.|
75712|Mount James Subgroup|73214|6|Mentioned|p974 Fig.1|Palaeoproterozoic|Palaeoproterozoic|||Pooranoo Metamorphics||||
75716|Mount Joanna Granodiorite|73596|6|Mentioned|p1165, 1170|Neoarchean|Neoarchean|Kalgoorlie-Kurnalpi Rift. Presented as the informal Mount Joanna granodiorite.|2939 +/- 6 Ma (Dunphy et al., 2003).|||||
34373|Mount Jope Supersequence|22682|5|Briefly described|Fig20,p29|Archean|Archean|2725-2681 Ma. Hamersley Province||||||07-NOV-08
34373|Mount Jope Supersequence|61254|6|Mentioned|p258 Fig.2.|Neoarchean|Neoarchean||||Includes the Tumbiana Sequence and the Maddina Sequence.|||24-APR-20
34373|Mount Jope Supersequence|64724|5|Briefly described|p43|Neoarchean|Neoarchean|Hamersley Basin sedimentary sequence. Age of ~2730-2715 Ma from Blake (1993, 2001).||||||
34373|Mount Jope Supersequence|65825|6|Mentioned|p20.|Neoarchean|Neoarchean|Named by Blake and Barley (1992), referring to rocks included in the Fortescue Group.||||||
34373|Mount Jope Supersequence|65827|6|Mentioned|p33 Fig.6|||Shown as equivalent to redefined Maddina (MJS2) and Tumbiana (MJS1) Formations.||||||21-JAN-22
34373|Mount Jope Supersequence|66685|6|Mentioned|p217|Archean|Archean|Blake and Barley (1992).||||||
23821|Mount Joseph Migmatite|24173|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Age: 1861 +/- 5Ma. The Marboo Formation forms a part of the migmatite in the West Kimberley||||||07-NOV-08
23821|Mount Joseph Migmatite|42710|5|Briefly described|map legend|Proterozoic||||||||
23821|Mount Joseph Migmatite|42811|5|Briefly described|p17|||||||||
23821|Mount Joseph Migmatite|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|Approx 1870-1865 Ma.||||||
23821|Mount Joseph Migmatite|50437|6|Mentioned|p2.4|||Intruded by: Paperbark Supersuite.||||||
23821|Mount Joseph Migmatite|63866|5|Briefly described|p132|||King Leopold Orogen. Thought to represent Marboo Formation which underwent granulite grade anatexis at 1861 +/- 5 Ma (Tyler et al, 1999).||||||
23821|Mount Joseph Migmatite|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|High-grade migmatitic granofels and anatectic granite.||||||09-DEC-08
23821|Mount Joseph Migmatite|64731|5|Briefly described|p164|Paleoproterozoic|Paleoproterozoic|In Hooper Complex of Halls Creek Orogen. Thought to represent metamorphosed Marboo Formation.||||||12-APR-12
23821|Mount Joseph Migmatite|69099|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||High-grade migmatitic granofels and anatectic granite.|03-AUG-15
23821|Mount Joseph Migmatite|69165|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||High grade migmatitic granofels and anatectic granite.|
23821|Mount Joseph Migmatite|69634|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||High-grade migmatitic granofels and anatectic granite|
23821|Mount Joseph Migmatite|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province; Halls Creek Orogen; North Australian Craton.|>1872 Ma (Tyler et al., 1999).||||Psammitic and pelitic migmatite and granofels; quartz-K-feldspar-plagioclase-biotite-sillimanite-muscovite(-cordierite-garnet-andalusite) rock; anatectic granite.|
23821|Mount Joseph Migmatite|70154|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv.|1864-1872 Ma||||Psammitic and pelitic migmatite and granofels; quartz--K-feldspar--plagioclase--biotite--sillimanite--muscovite(--cordierite--garnet--andalusite) rock; anatectic granite.|
23821|Mount Joseph Migmatite|70812|6|Mentioned|p3|||||||||
23821|Mount Joseph Migmatite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyp_lut.csv and geochron files.|1872+\-9 to 1864 Ma (isotopic, inferred)|Unit of Marboo Formation.|||Psammitic and pelitic migmatite and granofels; quartz-K-feldspar-plagioclase-biotite-sillimanite-muscovite(-cordierite-garnet-andalusite) rock; anatectic granite|
23821|Mount Joseph Migmatite|71397|5|Briefly described|p2|Orosirian|Orosirian|Geological province: Western Zone, Lamboo Province, Halls Creek Orogen. Oldest exposed rocks in the Western Zone, Lamboo Province. Metasedimentary rocks metamorphosed to greenschist to granulite facies.||||||
23821|Mount Joseph Migmatite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Central Zone, Halls Creek Orogen.|Max age 1872+/-9 ma, min age ~1864 Ma.|Marboo Formation|||Psammitic and pelitic migmatite and granofels; quartz--K-feldspar-plagioclase-biotit--sillimanite-muscovite(-cordierite-garnet-andalusite) rock; anatectic granite.|
23821|Mount Joseph Migmatite|72437|5|Briefly described|p14, p130|||Hooper Complex. One analysis is presented herein.||||Equivalent to the Marboo Formation.|High-grade metamorphic rocks.|
23821|Mount Joseph Migmatite|73089|6|Mentioned|p33|Orosirian|Orosirian|Lamboo Province, Western Zone. Dominantly Paleoproterozoic detritus[?].|c. 1875-1855 Ma||||Includes metasedimentary units.|
75885|Mount Kenneth Suite|68287|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Shown as younger than Meeline Suite.|< 2813 Ma|Of the Annean Supersuite.|||Metagranitic rock, locally sheared with abundant rafts and lenses of sheared quartzite, psammite, pelite; quartz-feldspar porphyritic rock, as dykes; metamorphosed.|
75885|Mount Kenneth Suite|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane. Hornblende-biotite granodiorite U-Pb zircon age:  2811 +/- 7 Ma as the magmatic crystallization age. See geochron file 193967.1.pdf. |2815-2800 Ma|Oldest granitic suite of Annean Supersuite|Includes 12 unnamed units.||Metagranitic rock; Gneissose metagranodiorite; Metamonzogranite; Metagranodiorite; Gneissose metamonzogranite; Granitic gneiss; Schistose metagranitic rock; Amphibole-rich metatonalite; Granodiorite; Monzogranite;|
75885|Mount Kenneth Suite|68698|5|Briefly described|p3-6, p9, p14-16, p18-19, p27-28|Mesoarchean|Mesoarchean|These plutons are thought to represent local melts, derived from tholeiitic sources, generated by the thermal effects of the Meeline and Boodanoo Suites. Geochemistry is discussed in some detail. Contemporaneous with felsic volcanic succcessions eg Kantie Murdanna Volcanics.|c.2815-2800 Ma.|Annean Supersuite.||Intrudes Meeline and Boodanoo Suites and Windimurra Igneous Complex.||
75885|Mount Kenneth Suite|69014|6|Mentioned|Map Legend|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane. Includes 2 unnamed facies.|2815-2800 Ma|Of the Annean Supersuite.|||Includes granodiorite and tonalite.|30-APR-14
75885|Mount Kenneth Suite|69583|4|Described|p49, p51, p53, p56-57, p99, p101, p103|Mesoarchean|Mesoarchean|See also p105; Plate 2. Ivanic et al. (2012). Murchison Domain, Youanmi Terrane, Yilgarn Craton. Appears also as Mt Kenneth Suite.|c.2815-2800 Ma.|Annean Supersuite.||Intruded the Meeline and Boodanoo Suites.|Metagranitic rock, with abundant rafts and lenses of sheared quartzite, psammite and pelite; metagranitic rock, locally sheared; metatonalite.|
75885|Mount Kenneth Suite|69584|6|Mentioned|p2|Mesoarchean|Mesoarchean|Meekatharra area. Appears as Mt Kenneth Suite.|||Courlbarloo Tonalite|||
75885|Mount Kenneth Suite|69586|5|Briefly described|p22|Mesoarchean|Mesoarchean|Murchison Domain.||Annean Supersuite.||||
75885|Mount Kenneth Suite|69626|5|Briefly described|map legend|Archean|Archean|Detailed lithology in legend. Murchison Domain, Youanmi Terrane, Yilgarn Craton||Annean Supersuite|||Amphibolitic metadolerite with metagabbro rafts; (meta)granodiorite; (meta)granitic rocks; gneissose metagranodiorite with ultramafic schist rafts; (meta)monzogranite; granitic gneiss; syenogranitic schist; metatonalite; microdiorite.|
75885|Mount Kenneth Suite|69744|6|Mentioned|p254||||c.2800 Ma.|||||
75885|Mount Kenneth Suite|70020|5|Briefly described|p113,118,129|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton. HFSE-enriched granitic rocks, similar geochemical characteristics to Yaloginda Formation and Kantie Murdana Volcanics Member.||Unit af Annean Supersuite.|Includes Courlbarloo tonalite.|Overlain by Culculli Suite.||
75885|Mount Kenneth Suite|70030|5|Briefly described|p192|Mesoarchean|Mesoarchean|Geological province: Murchison Domain, Yilgarn Craton.||Unit of Annean Supersuite.||||
75885|Mount Kenneth Suite|70140|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Three un-named facies are mapped separately.||Annean Supersuite.|Courlbarloo Tonalite.||Undivided: tonalite and metatonalite interlayered with metagranodiorite. Fine-grained felsic dykes, locally quartz and/or feldspar-phyric; granitic rock, includes deeply weathered rock; hornblende tonalite, locally weakly deformed; all metamorphosed.|
75885|Mount Kenneth Suite|70332|6|Mentioned|p79, 82|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|c.2800 Ma.||||Metagranitic rocks.|
75885|Mount Kenneth Suite|70419|5|Briefly described|p3, p9-10, p12-14, p26 Fig.10|Mesoarchean|Mesoarchean|May be associated with the rhyolites of the Kantie Murdana Volcanics Member.|c.2813 Ma.|||Overlies and is intruded by the Windimurra Igneous Complex.|Metagranitic (granodioritic/tonalitic) rocks.|
75885|Mount Kenneth Suite|70770|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. The four facies are mapped separately.|2815-2800 Ma.|Annean Supersuite.|||Metagranitic rock, locally sheared; schistose metagranitic rock, locally strongly sheared; metagranodiorite to metamonzogranite with muscovite-rich patches and rafts of metagabbro; felsic dykes, locally quartz and/or feldspar-phyric, metamorphosed.|
75885|Mount Kenneth Suite|70796|4|Described|2_5m_interpgeop15_lut.csv|Neoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. Affected by the Yilgarn Craton granite magmatism (3010  2600 Ma); Youanmi Terrane events (3131  2600 Ma). See also 100k_geologyl_lut.csv, 100k_geologyp_lut.csv, 100k_geologysub_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 185995.1.pdf, 185996.1.pdf, 193967.1.pdf, 198209.1.pdf, 198210.1.pdf, Bungar100_2539_stratig.pdf, Challa100_2541_stratig.pdf, Coolamaninu100_2540_stratig.pdf, Wynyangoo100_2542_stratig.pdf, Youanmi100_2640_stratig.pdf. Various different lithologies are discussed briefly.|ca 2815 to 2800 Ma (inferred)|Annean Supersuite|Includes the Courlbarloo Tonalite.|Intrudes the Meeline and Boodanoo suites.|Metatonalitic rock with subordinate metagranodiorite and metamonzogranite; locally strongly deformed; typically weakly schistose. Metagranite, gneissose metagranodiorite, schistose metagranite, tonalite.|
75885|Mount Kenneth Suite|70830|5|Briefly described|p9-p10, p29-p30, p33, p51, p54-p55|Mesoarchean|Mesoarchean|Murchison Domain.|c. 2813 Ma|Annean Supersuite|||Tonalite, metagranite.|
75885|Mount Kenneth Suite|71159|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.||Annean Supersuite.|||Tonalite; granodiorite, typically with sparsely distributed biotite schlieren, locally with rafts of amphibolite, metamorphosed.|
75885|Mount Kenneth Suite|71168|5|Briefly described|p7, p59|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Hosts HFSE-enriched intrusive rocks. Interpreted to be the intrusive equivalent of the Yaloginda Formation.|c. 2815-2800 Ma|Annean Supersuite|Includes the Courlbarloo Tonalite.||Granitic rocks.|
75885|Mount Kenneth Suite|71269|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). Sample GSWA 185995 (biotite metagranite) yielded a weighted mean 207Pb/206Pb date of 2806+\-3 Ma, interpreted as the magmatic crystallization age of the granite. Sample GSWA 185996 (biotite-hornblende metagranite) yielded a weighted mean 207Pb/206Pb date of 2803+\-3 Ma, interpreted as the magmatic crystallization age of the granite. Sample GSWA 193967 (hbl-bt granodiorite) yielded a weighted mean 207Pb/206Pb date of 2811+\-7 Ma, interpreted as the magmatic crystallization age of the granite. Sample GSWA 198210 (foliated metamonzogranite) yielded a weighted mean 207Pb/206Pb date of 2809+\-2 Ma, interpreted as the magmatic crystallization age of the monzogranite. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 100k_geologysub_lut.csv.|2815-2800 Ma|Unit of Annean Supersuite.|Includes Courlbarloo Tonalite.|Intrudes into Meeline and Boodanoo suites.|Granodiorite, gneissose metagranodiorite and metamonzogranite: rafts of amphibole, ultramafic schist and sheared quartzite; tonalite; hornblende and amphibole-rich metatonalite; sheared, metamorphosed.|
75885|Mount Kenneth Suite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Mesoarchean|Youanmi Terrane. ||Mount Kenneth Suite|Informally subdivided into 3 unnamed units.||Metagranitic rock, locally sheared with abundant rafts and lenses of sheared quartzite, psammite, and pelite. some includes deeply weathered rocks. Phenocrystic tonalite, locally sheared; includes rafts of amphibolite; metamorphosed.|
30208|Mount Kinahan Sandstone|22496|3|Fully described|p10||Neoproterozoic|Previously Mount Parker Sandstone. Of the Ruby Plains Group.  Geological Province:  Wolfe Basin.||||||12-AUG-04
30208|Mount Kinahan Sandstone|22777|5|Briefly described|Map|||Ruby Plains Group, Wolfe Basin||||||
30208|Mount Kinahan Sandstone|23314|4|Described|332|||Mount is Mt. in text.||||||
30208|Mount Kinahan Sandstone|23621|2|Defined|p55 Appendix|Cryogenian|Tonian|See also page 33, 9 table 1. Type section included. Of Ruby Plains Group. Overlying unit Eliot Range Dolomite. Underlying unit Olympio Formation. Geological Province: Wolfe Basin. Max. thickness: 150 m.||||||
30208|Mount Kinahan Sandstone|23622|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Ruby Plains Group. Geological Province: Wolfe Basin.||||||
30208|Mount Kinahan Sandstone|24173|4|Described|p24, p11 Tb.2|Tonian|Tonian|Of the Ruby Plains Group. Overlain by Eliot Range Dolomite; unconformably overlies Olympio Formation. Geological Province: Wolfe Basin. Max Thickness: 150m. Previously mapped as part of Mount Parker Sandstone.||||||06-APR-05
30208|Mount Kinahan Sandstone|43299|5|Briefly described|Map Legend||Neoproterozoic|of Duerdin Group.[Changed to Ruby Plains Group on later edition]||||||
30208|Mount Kinahan Sandstone|43303|5|Briefly described|Map Legend||Neoproterozoic|of Ruby Plains Group.||||||
30208|Mount Kinahan Sandstone|44868|5|Briefly described|Map Legend||Phanerozoic|||||||
30208|Mount Kinahan Sandstone|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Ruby Plains Group. Geological Province: Wolfe Creek Basin. Quartz sandstone.||||||03-NOV-04
30208|Mount Kinahan Sandstone|62453|6|Mentioned|p16|||Geological Province: Wolfe Creek Basin.||||||
30208|Mount Kinahan Sandstone|65338|6|Mentioned|p59.|||Wolfe Basin. Considered by Walter and Veevers (2000) to correlate with Vaughan Springs Quartzite.||||||
30208|Mount Kinahan Sandstone|68733|5|Briefly described|p189 Fig.8, p190|Cryogenian|Cryogenian|Written as Mt Kinahan Sandstone in text. Wolfe Basin.||Of the Ruby Plains Group.||Correlated with Heavitree Quartzite and Jasper Gorge Sandstone.||05-DEC-17
30208|Mount Kinahan Sandstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Cryogenian|Cryogenian|Wolfe Creek Basin||Ruby Plains Group|||Quartz sandstone.|03-AUG-15
30208|Mount Kinahan Sandstone|69165|5|Briefly described|100k_interpgeop_lut.csv|Neoproterozoic|Neoproterozoic|||Ruby Plains Group|||Quartz sandstone.|
30208|Mount Kinahan Sandstone|69634|4|Described|100k_interpgeop_lut.csv|Cryogenian|Cryogenian|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1.|830-810 Ma (Inferred)|Unit of Ruby Plains Group.|||Quartz sandstone|
30208|Mount Kinahan Sandstone|70154|5|Briefly described|100k_interpgeop_lut.csv|Cryogenian|Neoproterozoic||810-1000 Ma|Ruby Plains Group|||Quartz sandstone.|
30208|Mount Kinahan Sandstone|71267|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1000-720 Ma (inferred)|Unit of Ruby Plains Group.|||Quartz sandstone, minor conglomerate; distinctive stromatolites present|
31403|Mount Leake Formation|12099|6|Mentioned|p685|Paleoproterozoic|Paleoproterozoic|||Unit in Earaheedy Group.||||04-MAR-13
31403|Mount Leake Formation|23529|5|Briefly described|p10|Paleoproterozoic|Paleoproterozoic|Age: 1785+/-11Ma (SHRIMP U-Pb).||||||15-DEC-08
31403|Mount Leake Formation|23589|5|Briefly described|p6 Table 2|||1785+/-11 Ma (SHRIMP U-Pb zircon). Of Earaheedy Group. Geological Province: Earaheedy Basin.||||||
31403|Mount Leake Formation|23597|5|Briefly described|p19|Statherian|Statherian|Age: 1785+/-11 Ma (SHRIMP). Of Earaheedy Group.||||||
31403|Mount Leake Formation|23744|5|Briefly described|p11|Statherian|Statherian|Age: 1785+/-11 Ma. Of Earaheedy Group. Geological Province: Earaheedy Basin.||||||
31403|Mount Leake Formation|23747|4|Described|p16|||Of Earaheedy Group.||||||
31403|Mount Leake Formation|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Earaheedy Group. Geological Province: Earaheedy Basin.||||||
31403|Mount Leake Formation|23749|4|Described|p14|Proterozoic|Proterozoic|Of Earaheedy Group. Geological Province: Earaheedy Basin. Max. thickness: 50 m.||||||
31403|Mount Leake Formation|23750|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Earaheedy Group. Geological Province: Earaheedy Basin.||||||
31403|Mount Leake Formation|24028|6|Mentioned|p289 Fig. 2|||||||||
31403|Mount Leake Formation|43238|5|Briefly described|p7|||Earaheedy Group.||||||15-DEC-08
31403|Mount Leake Formation|50188|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Age: 1785 +/- 11Ma derived from detrital zircons (SHRIMP). On PEAK HILL 1:250K sheet.||||||07-NOV-08
31403|Mount Leake Formation|50222|5|Briefly described|p320 Fig. 3|Paleoproterozoic|Paleoproterozoic|Glauconite.  Age: 1.78Ga and 1.83Ga.||||||07-NOV-08
31403|Mount Leake Formation|62289|4|Described|plate 1, p32|Palaeoproterozoic|Palaeoproterozoic|Of Earaheedy Group; quartz arenite, locally glauconitic; basal jasperoidal chert and green chert breccia may be a palaeoregolith material (silcrete?); straddles the Goodin Fault, indicating that it was deposited well after the tectonic juxtaposition of the Bryah and Yerrida Groups. Age: c. 1 785 Ma. Geol. Prov: Earaheedy Basin.||||||
31403|Mount Leake Formation|63866|4|Described|p165, p167, p175|Statherian|Statherian|SHRIMP age is interpreted as constraining the maximum depositional age for this formation. May be equivalent to the Yelma Formation. A second sample from this formation yielded a SHRIMP U-Pb age of  1832 +?- 37 Ma (Nelson, 1997) and is interpreted to represent the maximum age of deposition.|1785 +/- 11 Ma (SHRIMP U-Pb, Nelson, 1997)|||Unconformably overlies the Bryah Group. Equivalent to the Earaheedy Group.||
31403|Mount Leake Formation|64580|4|Described|map legend||Paleoproterozoic|Quartz arenite; locally glauconitic.||||||15-DEC-08
31403|Mount Leake Formation|65419|1|Redefined|p29, p37, pp48-50.|Paleoproterozoic|Paleoproterozoic|Originally the Mount Leake Sandstone of Gee (1979, 1987) and Elias et al. (1982); revised by Gee and Grey (1993); renamed and redefined in this study. Named after Mount Leake, the type area. Up to 50 m thick. Age from detrital zircons. Coeval with Yelma Formation.|1785 +/- 11 Ma (Nelson, 1997).|Unit in Earaheedy Group.||Unconformably overlies the Bryah and Yerrida Groups.|Silica-cemented, fine-grained, well-sorted and well-rounded orthoquartzitic sandstone; interbedded shale; thick irregular beds of intraformational conglomerate; stromatolitic chert; local basal chert breccia, quartz arenite and fine pebble beds.|
31403|Mount Leake Formation|66427|5|Briefly described|p42, p44 Tb.2|||Mount Leake outlier; straddles the Goodin Fault that separates Yerrida and Bryah Basins. Contains detrital zircon from sandstone aged 1785 +/- 11 Ma (U-Pb SHRIMP; Nelson, 1997).|1573 Ma (glauconite K-Ar; Butt et al., 1977).|||Possible correlative of the Yelma Formation.|Consists of a basal jasperoidal chert and green chert breccia about 2 m thick, followed upward by a ferruginous sandstone layer and by beds of cross-bedded, locally glauconitic, quartz arenite.|
31403|Mount Leake Formation|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic||||||Quartz arenite; locally glauconitic|
31403|Mount Leake Formation|69166|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Quartz arenite; locally glauconitic.|
31403|Mount Leake Formation|69596|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||||||
31403|Mount Leake Formation|70795|4|Described|500k_interpgeop14_lut.csv|Mesoproterozoic|Paleoproterozoic||1785-1000 Ma||||Quartz arenite; locallly glauconitic.|
31403|Mount Leake Formation|70796|4|Described|2_5m_interpgeop15_lut.csv|Mesoproterozoic|Paleoproterozoic|Of the Edmund Basin, Capricorn Orogen. Affected by the following events: Mulka Tectonic Event (570  570 Ma); Edmundian Orogeny (1026  954 Ma); Mutherbukin Tectonic Event (1321  1171 Ma). See also 500k_interpgeop14_lut.csv.|ca. 17851000 Ma (inferred)||||Quartz arenite; locally glauconitic.|
31403|Mount Leake Formation|70804|5|Briefly described|p6, plate 1|Statherian|Statherian||1785 +/- 11 Ma (Nelson, 1997)|Earaheedy Group||Unconformably overlies the Bryah Group.||
31403|Mount Leake Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, greensand, crystalline carbonate, chert|
31403|Mount Leake Formation|71269|5|Briefly described|GEOL_LUT_CSV files|Mesoproterozoic|Paleoproterozoic|Of Edmund Basin. Events: Mulka Tectonic Event (570-570 Ma); Edmundian Orogeny (1026-954 Ma); Mutherbukin Tectonic Event (1321-1171 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv.|1785-1000 Ma (inferred)||||Quartz sandstone, glauconitic in places, silicified stromatolitic carbonate, chert breccia and jasperoidal chert|
31403|Mount Leake Formation|71484|6|Mentioned|p125|||Geological province: Of Edmund and Collier basins.|||||Quartz arenite, locally glauconitic.|30-AUG-19
31403|Mount Leake Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Paleoproterozoic|Edmund Basin.|||||Quartz arenite; locally glauconitic.|
79015|Mount Leonora Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||2817 - 2753 Ma (inferred).||||Felsic schist derived from volcanic rock, felsic volcanic and volcaniclastic rocks. Oligomictic conglomerate, conglomerate with minor sandstone and siltstone, sandstone, siltstone, shale and chert; all metamorphosed.|
79015|Mount Leonora Formation|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).  See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2817-2753 Ma (inferred)|||Overlain by Marshall Pool Subgroup.|Felsic volcanic and volcaniclastics: metamorphosed; schist; felsic, qtz-andalusite, qtz-ms; sandstone, siltstone, shale, chert; oligomictic conglomerate: metamorphosed.|
79015|Mount Leonora Formation|73596|6|Mentioned|p1159, 1162-1163, 1165, 1170|Mesoarchean|Mesoarchean|Leonora Inlier, Kalgoorlie Terrane.|2817 +/- 6 Ma (MDA: Baggott, 2006).|||Conformably overlies Trevors Bore Formation. Is overlain by Hangover Basalt (Marshall Pool Subgroup) paraconformably.|Volcano-sedimentary rocks: greywacke, quartzite, and chlorite schist.|
38644|Mount Lucky Conglomerate|23786|5|Briefly described|p5|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
80040|Mount Malcolm Granite|67268|6|Mentioned|p30|||Occurs in the Eastern and Western margins of the Mount Malcolm mapping region. The rocks are shown simply as 'Granitic intrusions' on Outcrop Map 2: geology of Mount Malcolm.||||||22-SEP-17
36130|Mount Manypeaks granite|23514|5|Briefly described|p102 Fig.1|Mesoproterozoic|Mesoproterozoic|||||||
74449|Mount McRae Shale and Mount Sylvia Formation|69569|6|Mentioned|p285 Fig.1|||East Pilbara Terrane. Appears in Fig.1 as Mt McRae and Mt Sylvia.||Hamersley Group.||||
74449|Mount McRae Shale and Mount Sylvia Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Hamersley Basin.||Hamersley Group, lower|||Mudstone, siltstone, chert, banded iron-formation, and dolomite; metamorphosed.|
29294|Mount Minnie Group|22484|6|Mentioned|p72|||Mount is written Mt in text||||||
29294|Mount Minnie Group|22716|5|Briefly described|p229|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
29294|Mount Minnie Group|23325|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
29294|Mount Minnie Group|23485|6|Mentioned|p24|||Geological Province: Ashburton Basin.||||||
29294|Mount Minnie Group|23525|6|Mentioned|p24|||||||||
29294|Mount Minnie Group|23570|6|Mentioned|p18|||||||||
29294|Mount Minnie Group|23575|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Overlying unit Bresnahan Group.||||||
29294|Mount Minnie Group|24183|5|Briefly described|p2 Fig.1, p6|Paleoproterozoic|Paleoproterozoic|Geological Province: Ashburton Basin.||||||07-NOV-08
29294|Mount Minnie Group|24203|5|Briefly described|p292 Fig. 7|||Age: 1800 Ma. Geological Province Carnarvon Basin. Mount is Mt in text.||||||22-MAY-08
29294|Mount Minnie Group|24544|4|Described|p38, 48||Paleoproterozoic|Unconformably overlies Ashburton Formation and Capricorn Group. Unconformably overlain by Bresnahan Group. Max. thickness: 2600 m. Geological Province: Ashburton Basin.||||||07-NOV-08
29294|Mount Minnie Group|24602|5|Briefly described|p854 Fig. 1|||Geological Province: Ashburton Fold Belt.||||||
29294|Mount Minnie Group|24607|6|Mentioned|p968 Fig. 1|||Mount is Mt. in text. See also Mount Minnie Formation.||||||30-NOV-10
29294|Mount Minnie Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
29294|Mount Minnie Group|31393|6|Mentioned|Pl.25|||||||||
29294|Mount Minnie Group|33544|6|Mentioned|p30|||See also Plates 1 & 2. Middle Proterozoic||||||
29294|Mount Minnie Group|34066|5|Briefly described|p9|||M.Prot.||||||
29294|Mount Minnie Group|34834|6|Mentioned|p219|||||||||
29294|Mount Minnie Group|35260|6|Mentioned|p5|||Map legend||||||
29294|Mount Minnie Group|35976|6|Mentioned|p107|||||||||
29294|Mount Minnie Group|36551|6|Mentioned|p92|||||||||
29294|Mount Minnie Group|36883|4|Described|p145|||||||||
29294|Mount Minnie Group|36884|6|Mentioned|p147|||||||||
29294|Mount Minnie Group|36891|6|Mentioned|p442|||||||||
29294|Mount Minnie Group|37299|6|Mentioned|p88|||||||||
29294|Mount Minnie Group|37422|6|Mentioned|p8|||||||||
29294|Mount Minnie Group|37577|6|Mentioned|p6|||||||||
29294|Mount Minnie Group|39427|6|Mentioned|p4|||||||||
29294|Mount Minnie Group|40089|6|Mentioned|p11|||See also P176||||||
29294|Mount Minnie Group|40369|6|Mentioned|Fig.1|||||||||
29294|Mount Minnie Group|40935|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
29294|Mount Minnie Group|40937|6|Mentioned|p5|||See also P81||||||
29294|Mount Minnie Group|41360|6|Mentioned|p192|||||||||
29294|Mount Minnie Group|42148|5|Briefly described|p686|||||||||
29294|Mount Minnie Group|42260|4|Described|p98|||||||||
29294|Mount Minnie Group|42435|6|Mentioned|p46|||||||||
29294|Mount Minnie Group|42471|6|Mentioned|p14|||||||||
29294|Mount Minnie Group|42744|6|Mentioned|p8|||||||||
29294|Mount Minnie Group|43119|6|Mentioned|p18|||||||||
29294|Mount Minnie Group|43290|6|Mentioned|p10||Proterozoic|||||||
29294|Mount Minnie Group|43561|5|Briefly described|Fig.3,1434,1436,1438|||||||||
29294|Mount Minnie Group|44477|4|Described|p.12-13, Table 1||Proterozoic|SF/50-6.||||||
29294|Mount Minnie Group|44478|14|Not recorded|map legend||Proterozoic|||||||
29294|Mount Minnie Group|44481|5|Briefly described|map legend||Mesoproterozoic|||||||
29294|Mount Minnie Group|44867|5|Briefly described|Map Legend||Mesoproterozoic|||||||
29294|Mount Minnie Group|50216|5|Briefly described|p209|||Geological Province: Mount Minnie Basin.||||||
29294|Mount Minnie Group|50225|5|Briefly described|p386 Fig. 1|||||||||07-FEB-11
29294|Mount Minnie Group|50226|6|Mentioned|p415|||Conglomerate, sandstone and mudstone.||||||
29294|Mount Minnie Group|61276|6|Mentioned|p577 Fig.1|||||||||
29294|Mount Minnie Group|62129|6|Mentioned|p18|||||||||07-FEB-11
29294|Mount Minnie Group|63866|6|Mentioned|p151|||||||||
29294|Mount Minnie Group|64384|5|Briefly described|p48 Fig.40|||Part of the Minnie Creek Batholith.||||||07-FEB-11
29294|Mount Minnie Group|64580|4|Described|map legend||Paleoproterozoic|Quartz sandstone, conglomerate, siltstone and mudstone.||||||15-DEC-08
29294|Mount Minnie Group|64728|6|Mentioned|p94 Fig.1. |||||||||
29294|Mount Minnie Group|67201|6|Mentioned|p33 Fig.17|||||||||
29294|Mount Minnie Group|67855|5|Briefly described|p220-221, 211, 212, 224, 229, 230||Paleoproterozoic|Mount Minnie Basin. 1600m thick. Structural relationship indicate age younger than Boolaloo granodiorite and older than Bresnahan Basin. Fan delta deposits.|||Includes Brodagee Sandstone, Wabco Shale, Warramboo Sandstone.|||
29294|Mount Minnie Group|69003|5|Briefly described|p4, p25, p36|Paleoproterozoic|Paleoproterozoic|Capricorn Orogen. Sediments sourced mainly from upper Wyloo Group.||||Unconformably overlies Ashburton Formation.|Shallow-marine sandstone, pebbly sandstone, and conglomerate.|
29294|Mount Minnie Group|69028|5|Briefly described|Map Legend|Statherian|Statherian|Ashburton and Blair Basins. These three Formations are mapped as a single unit.|1800-1620 Ma.||Includes Brodagee Sandstone, Wabco Shale and Warramboo Sandstone.||Includes quartz sandstone, conglomerate, siltstone, and mudstone.|07-MAY-14
29294|Mount Minnie Group|69080|6|Mentioned|p684|||Pilbara Craton.|||||Sandstone and siltstone.|
29294|Mount Minnie Group|69185|4|Described|GEOL_LUT_CSV files||Paleoproterozoic|Of Mount Minnie Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|||||Undivided, quartz sandstone, conglomerate, siltstone and mudstone|
29294|Mount Minnie Group|69387|6|Mentioned|p19|||Boora Boora Zone, Gascoyne Province. Structural fabric diagram.||||||
29294|Mount Minnie Group|69596|6|Mentioned|p5|Statherian|Statherian|Southern Pilbara.||||||
29294|Mount Minnie Group|70327|6|Mentioned|p3|||||||||
29294|Mount Minnie Group|70814|6|Mentioned|p32, p35 fig 19, p74|||||||||
29294|Mount Minnie Group|70826|6|Mentioned|p5 tbl 2, p10|Paleoproterozoic|Paleoproterozoic|Mount Minnie Basin.||||||20-APR-20
29294|Mount Minnie Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||shale, conglomerate, sandstone, mudstone|
29294|Mount Minnie Group|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Mount Minnie Basin.|||||Quartz sandstone, conglomerate, siltstone and mudstone.|
29294|Mount Minnie Group|72259|6|Mentioned|p3|Statherian|Statherian||ca. 1800-1600 Ma|||||
29294|Mount Minnie Group|72712|6|Mentioned|p3.|||Included in Hamersley province.||||||
29294|Mount Minnie Group|72758|5|Briefly described|p4 Fig.1, p9-10 Tb.1, p30, p37, p48-49.|Paleoproterozoic|Paleoproterozoic|This group is c. 1600m thick. Age poorly known. Must be younger than Ashburton Formation (clasts in basal beds). Inferred to be deposited between D1 and D2 deformation. Interpreted as an association of fan-delta deposits laid down in a single basin, or in separate, unconnected sub-basins (Daniels, 1970).|Max age: 2000 Ma. Min age: ~1680 Ma||Brodagee Sandstone, Wabco Shale, Warramboo Sandstone.|Unconformably overlies Ashburton Formation. Unconformably underlies Bangemall Group, Phanerozoic rocks.|Silicified conglomerate, sandstone, and mudstone.|
34389|Mount Minnie-Mount Blair Supersequence|22682|5|Briefly described|Fig21,p31|Statherian|Statherian|Age: 1771-1724 Ma. Ashburton Province.||||||03-MAR-10
78643|Mount Monger Intrusion|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton|||||Gabbro; relict cumulate texture; metamorphosed.|06-AUG-15
78643|Mount Monger Intrusion|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Gabbro; relict cumulate texture; metamorphosed.|
78643|Mount Monger Intrusion|71270|4|Described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton.|||||Gabbro; relict cumulate texture; metamorphosed|
23826|Mount Newman Member|22689|6|Mentioned|138 fig 1|Paleoproterozoic|Archean|Of Marra Mamba Iron Formation, Hamersley Basin.  SHRIMP age 2597+/-5 Ma.  Mount as 'Mt' in text||||||07-NOV-08
23826|Mount Newman Member|22701|4|Described|p40|Archean|Archean|Marra Mamba Iron Formation, Hamersley Group, Hamersley Basin. 2600 Ma.||||||07-NOV-08
23826|Mount Newman Member|23046|5|Briefly described|171|||Mount as 'Mt' in text||||||
23826|Mount Newman Member|23126|4|Described|p382|||||||||
23826|Mount Newman Member|23536|5|Briefly described|p 427|||"Mt" used in text. Also see p 433||||||
23826|Mount Newman Member|24041|5|Briefly described|p493|Archean|Archean|Of Marra Mamba Iron Formation. Geological Province: Pilbara Craton.||||||08-APR-09
23826|Mount Newman Member|24533|5|Briefly described|p5 Table. 2|Archean|Archean|Of the Marra Mamba Iron Formation (Hamersley Group). Age: 2597 +/- 5Ma (SHRIMP).||||||07-NOV-08
23826|Mount Newman Member|24544|4|Described|p57 Fig.43|Archean|Archean|Of Marra Mamba Iron Formation. Overlies MacLeod Member. Overlain by West Angela Member of Wittenoom Formation. Banded iron-formation. Age: c. 2597 Ma.  Geological Province: Hamersley Basin.||||||07-NOV-08
23826|Mount Newman Member|39589|6|Mentioned|p158|||||||||
23826|Mount Newman Member|42112|5|Briefly described|p8|||See also Table 1||||||
23826|Mount Newman Member|42190|6|Mentioned|p276|||||||||
23826|Mount Newman Member|42471|5|Briefly described|p7|||of Marra Mamba Iron Formation.||||||
23826|Mount Newman Member|42495|5|Briefly described|p35|||||||||
23826|Mount Newman Member|42744|5|Briefly described|p4|||of Marra Mamba Iron Formation.||||||
23826|Mount Newman Member|43063|3|Fully described|p53|||of Marra Mamba Iron Formation||||||
23826|Mount Newman Member|43119|5|Briefly described|p9|||of Marra Mamba Iron Formation||||||
23826|Mount Newman Member|43210|5|Briefly described|Table 1 p3,p4.|||of Marra Mamba Iron Formation.||||||
23826|Mount Newman Member|43290|5|Briefly described|p6||Archean|of Marra Mamba Iron Formation.||||||07-NOV-08
23826|Mount Newman Member|44152|5|Briefly described|p179 Fig.2-155|||||Marra Mamba Iron Formation||Overlies Mount MacLeod Member. Is overlain by Wittenoom Dolomite.|BIF, shale.|
23826|Mount Newman Member|60373|6|Mentioned|p145 Tb. 1|Archean|Archean|Of Marra Mamba Iron Formation.||||||23-JUN-09
23826|Mount Newman Member|60706|5|Briefly described|p623 Fig.2|||Of the Marra Mamba Iron Formation (Hamersley Group). Geological Province: Hamersley Basin.||||||
23826|Mount Newman Member|62129|3|Fully described|p9|Archaean|Archaean|Of Marra Mamba Iron Formation. Thickness: 60m. Geological Province: Hamersley Basin. Dominantly BIF with thin shale intervals.||||||07-FEB-11
23826|Mount Newman Member|63153|6|Mentioned|p1359, p1361 Fig.2, p1363, p1365-1373, |||Most productive part of the Marra Mamba Iron Formation. Average thickness 54 m. Often abbreviated to Newman Member in text.||Unit in Marra Mamba Iron Formation.||Overlies MacLeod Member. Is overlain by West Angela Member (Wittenoom Formation).|High-grade martite-limonite ore.|
23826|Mount Newman Member|64384|5|Briefly described|p35 Tb. 6|||Upper member of Marra Mamba Iron Formation (Hamersley Group). Overlies MacLeod Member. Geological province: Hamersley Basin. BIFinterbedded with 18 thin shale horizons; some chert.||||||07-FEB-11
23826|Mount Newman Member|65683|5|Briefly described|p799, p800, p801 Fig2,p802|||Upper unit of Marra Mamba Iron Formation. Underlies West Angela Member of Wittenoom Formation; overlies MacLeod Member. Economically important unit: iron formation with abundant iron oxide mesobands.||||||08-MAR-12
23826|Mount Newman Member|66882|5|Briefly described|p118|Neoarchean|Neoarchean|Detrital zircons of the same age occur in Cook Gap Schist, Gawler Craton.|c.2600 Ma|Hamersley Group.|||Contains tuff bands.|
23826|Mount Newman Member|67056|5|Briefly described|p419 Fig.2, p439, p445. |||Magnetite-rich BIF macrobands alternate with non-IF carbonate and shale horizons; similar in style (but with higher iron) to the overlying Wittenoom Formation.||Unit in Marra Mamba Iron Formation.||Overlies MacLeod Member. Is overlain by Wittenoom Formation.||
23826|Mount Newman Member|67130|5|Briefly described|p3 fig 2|Neoarchean|Neoarchean||2597 Ma +/- 5 Ma|Marra Mamba Iron Formation||Overlies MacLeod Member, overlain by West Angela Member|Banded iron formation|
23826|Mount Newman Member|67201|5|Briefly described|p34 Fig.18|||Shown as Mount Newman Mbr.||Marra Mamba Iron Formation||||
23826|Mount Newman Member|67721|5|Briefly described|p37, p38 Fig.9|Neoarchean|Neoarchean|Approximately 65 m thick. Geochronology from tuff bands.|c. 2600 Ma (Trendall et al. 1998).|Of the Marra Mamba iron formation.||||
23826|Mount Newman Member|68035|5|Briefly described|p292 Fig 6|Neoarchean|Neoarchean|Hamersley Group, Hamersley Basin.|2597+/- 5 Ma|Of Marra Mamba Iron Formation.||Overlies MacLeod Member, overlain by West Angela Mmeber, Wittenoom Formation.|Banded iron formation.|
23826|Mount Newman Member|68280|6|Mentioned|p5|||||Marra Mamba Iron Formation|||Banded iron formation.|
23826|Mount Newman Member|69538|6|Mentioned|p516, p517 Fig.3, p524, p529 Fig.9|||See also p552, p576, p583-585. ||Unit in Marra Mamba Iron Formation.||||
23826|Mount Newman Member|71808|4|Described|vi, p10-p11, p19-p20, p48, p50, p53, |||Hamersley Province. Type section occurs in DDH275 (Blockley et al, 1993). Characterised by very pronounced podding, especially stacked pods compared with other BIFs of the group. Petrography is discussed. See also p55, p57, p60, p71-p72, p75, p83, p86, p87, p88, p90, p95, p117, p127, p130, p150, p152-p153, p173, p174, p221-p222, p232, p243, p246-p247.||Marra Mamba Iron Formation|||Stilpnomelane-rich (tuffaceous) shale and or poorly bedded rock after carbonate.|
23826|Mount Newman Member|72493|5|Briefly described|p30|||Hamersley Basin.||Marra Mamba Iron Formation.||Overlies McLeod Member. Is overlain by West Angelas Member (Wittenoom Formation).|BIF.|
23826|Mount Newman Member|72569|6|Mentioned|p2|||Of the Hamersley Basin.||Marra Mamba Iron Formation||||
23826|Mount Newman Member|73022|6|Mentioned|p3 Fig.2|||||Marra Mamba Iron Formation||Overlies the MacLeod Member, underlies the West Angela Member.|Banded iron formation, shale and minor Fe-chert.|
23826|Mount Newman Member|73290|5|Briefly described|p783-785, 797|||Hamersley Basin. Shown invariably as Mt Newman Member. Mineralogy and petrography described in detail.||Marra Mamba Iron Formation.||||
23826|Mount Newman Member|73538|6|Mentioned|p4|Neoarchean|Neoarchean|An age of 2597 +/- 5 Ma was reported by Trendall et al. (2004). [Written as Mt. Newman member].|2597 +/- 5 Ma|Marra Mamba Iron Formation||Underlain by the MacLeod Member. Overlain by the West Angela Member of the Wittenoom Formation.|Iron formation.|
31792|Mount Nyulasy Granite|22547|4|Described|p12|Orosirian|Orosirian|Of the Paperbark supersuite. Age: 1859 +/- 3 Ma.||||||14-NOV-06
31792|Mount Nyulasy Granite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.||||||07-NOV-08
31792|Mount Nyulasy Granite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
31792|Mount Nyulasy Granite|43853|5|Briefly described|Map Legend||Proterozoic|||||||
31792|Mount Nyulasy Granite|44230|5|Briefly described|Map Legend||Proterozoic|||||||
31792|Mount Nyulasy Granite|66845|4|Described|p537 Fig.3, p539 Tb.1, p540, p542 Fig.6|||Two cores (no. 30.1 and 5.1) gave 3260 Ma and 2009 Ma, indicating xenocrysts or inherited from source, however, Fig.6 states ages of 3261 and 2009 Ma; 44 analyses for interpreted magmatic crystallisation age.|interp. magm. cryst'n age 1859+/-3 Ma SHRIMP U-Pb|Paperbark supersuite|||porphyritic monzogranite|
31792|Mount Nyulasy Granite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Paperbark Supersuite|||Coarse-grained, rapakivi-textured monzogranite and syenogranite; subordinate medium- to coarse-grained, equigranular monzogranite.|03-AUG-15
31792|Mount Nyulasy Granite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Paperbark Supersuite|||Coarse-grained, rapakivi-textured monzogranite and syenogranite; subordinate medium- to coarse-grained, equigranular monzogranite.|
31792|Mount Nyulasy Granite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone.|1859-1859 Ma (Isotopic)|Unit of Paperbark Supersuite.|||Coarse-grained, rapakivi-textured monzogranite and syenogranite; subordinate medium- to coarse-grained, equigranular monzogranite|
31792|Mount Nyulasy Granite|70154|6|Mentioned|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1859 Ma|Paperbark Supersuite||||
31792|Mount Nyulasy Granite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (183 -1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1859+\-3 Ma (isotopic)|Unit of Paperbark Supersuite.|||Coarse-grained, rapakivi-textured monzogranite and syenogranite; subordinate medium- to coarse-grained, equigranular monzogranite|
31792|Mount Nyulasy Granite|72437|5|Briefly described|p88-89|||Lamboo Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Biotite monzogranite.|
76740|Mount Palgrave Group|67244|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Mapped as four separate but un-named sub-units.|1077 - 1063 Ma.|Unit in Bentley Supergroup.|||Rhyolitic and trachydacitic volcanic sandstone, siltstone and mudstone, contains fiamme; minor mafic volcanic rocks; ignimbrite; rhyolite and trachydacite, spherulitic, perlitic or massive, intruded by / included in quartz syenite and syenogranite.|11-APR-12
76740|Mount Palgrave Group|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||1078 - 1063 Ma.|Unit in Bentley Supergroup.|||Rhyolite and trachydacite, rounded amygdales to 4 cm; rhyolitic and trachydacitic sandstone and siltstone containing fiamme; ignimbrite; aphyric rhyolite and trachydacite, spherulitic, perlitic or massive; minor mafic volcanic rocks.|
76740|Mount Palgrave Group|67375|5|Briefly described|pp8-9 Fig.5, p38 Table 1, p39, pp44-46. |Mesoproterozoic|Mesoproterozoic|Palgrave area, Talbot Sub-basin, Musgrave Region. See also references to Palgrave Group (p20 Fig.11). Minimum age from dataing of a sample of a massive feldspar-phyric rhyolite positioned above the porphyritic marker horizon in the upper Mount Palgrave Group. A microgranite intruding into a higher part of the sequence is dated at 1064 +/-7 Ma.|1077-1063 Ma.|Unit in Bentley Supergroup.||Intruded by Winburn Granite.|Dacitic to rhyolitic volcanic and pyroclastic rocks; minor intercalations of tholeiitic basalt and sedimentary rocks including diamictite, siliciclastic conglomerates, sandstones and mudstones rich in volcanogenic detritus.|02-DEC-13
76740|Mount Palgrave Group|67553|4|Described|p8,11,17,21,40-44,46,59,63,93-94|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Talbot Sub-basin, Bentley Sub-basin. [Referred to as Palgrave Group on p21]. Series of extremely violent, high-energy eruptions of compositionally evolved rhyolitic magmas and less voluminous tholeiitic mafic magmas. Lower section age constrained by 1077+\-6 Ma Mount Eliza granophyre (GSWA 174662) and 1064+\-7 Ma post depositional porphyry intrusion (GSWA 194637). Deformation, uplift, erosion, and deposition of diamictite at the base of the upper part of Mount Palgrave Group 1065-1063 Ma. Glyde Formation juxtaposed against diamictite in the upper Mount Palgrave Group as a result of NW-trending faulting and reactivation of earliers sub-volcanic block faults at <1055+\-10 Ma. Intrusive rocks include dykes, sills, and irregular small bodies of feldspar and quartz-feldspar-phyric rhyolitic microgranites, quartz diorites, dolerites.|1077-1060 Ma|Unit of Bentley Supergroup.|||Pherulitic and perlitic trachyrhyolites and rhyolites and minor basalts and clastic rocks, overlain by felsic volcanics, pyroclastic and siliciclastic rocks.|
76740|Mount Palgrave Group|68995|6|Mentioned|p3-p4, p7-10, p12-14, p18, p20-21, p24|Stenian|Stenian|Talbot Sub-basin. Age based on the Giles Event which occurred as this unit was deposited. Stratigraphy is right way up. Rocks of this Group generally dip shallowly, but locally steep dip is also present. Estimated to be more than 4500m thick, based on best exposure in the northeast of the Talbot Sub-basin. Geochemistry discussed. See also p26, p28-29, p31 Fig.17, p35 Fig.20, p43, p45-46, p49 Fig.25, p56-57.|c. 1085-1040 Ma|Bentley Supergroup|Eliza Formation, Scamp Formation, Mount Waugh rhyolite|Overlies (or is intruded by) the Winburn Granite. Overlain by the Kaarnka Group and Pussy Cat Group.||
76740|Mount Palgrave Group|68996|5|Briefly described|p5,7,32,39,34,36-39,47,50,52,57,62,64,65|Mesoproterozoic|Mesoproterozoic|Intruded by granitic dykes 1068+/-6 Ma, 1052+/-11 Ma. Misspelt as Palgrave Group p52.|1064 +/- 7 Ma (SHRIMP)|Bentley Supergroup|Includes Scamp Formation||Dacitic to rhyolitic volcanic rocks, with minor intercalations of basalt and sedimentary rocks.|
76740|Mount Palgrave Group|69003|5|Briefly described|p51-52|Mesoproterozoic|Mesoproterozoic|Palgrave and Scamp areas, Talbot Sub-basin.|c.1070 - 1063 +/- 8 Ma.|||Is intruded by, or overlies, Winburn Granite.|Dominantly rhyolitic volcanic and pyroclastic rocks, with minor intercalations of basalt and sedimentary rocks.|
76740|Mount Palgrave Group|69009|5|Briefly described|Map Legend|Stenian|Stenian|Bentley Basin.|1077-1063 Ma|Of the Bentley Supergroup.|Includes Mount Waugh Formation, Scamp Formation, and Eliza Formation.||Comprises rhyolite; clast- to matrix-supported conglomerate; rhyolitic volcaniclastic sandstone; rhyolite lava flows, minor subvolcanic sills, and pyroclastic rocks - interlayered with aphyric rhyolite or volcanic siltstone.|
76740|Mount Palgrave Group|69091|5|Briefly described|p30 Fig.3.5, p52 Fig.4.1, see comments||Mesoproterozoic|Talbot Sub-basin. Up to 4500 m of volcanic stratigraphy. Very unusual size (extent and volume) and facies association of volcanic rocks. Misspelled as Palgrave Group on p30 Fig.3.5, p81 Fig.4.17, p108 Fig.5.9, p117 Fig.5.15, p119 Fig.5.16, p146, p174 Fig.9.5, p177 Fig.9.6. See also p54 Fig.4.2, p59 Fig.4.6, p71 Fig.4.14, p75-76, p81 Fig.4.17, p83, p103 Fig.5.6, p106-109 Figs.5.7-10, p115 Fig.5.14, p117 Fig.5.15, p119 Fig.5.16, p131 Fig.6.1, p133, p134 Fig.6.2, p144, p146, p174 Fig.9.5, p177 Fig.9.6, p200 Fig.10.2, p204-206.|Max: c. 1070 Ma.|Bentley Supergroup|Mount Waugh rhyolite, Scamp Formation, Eliza Formation|Is overlain by Kaarnka Group and Pussy Cat Group; is intruded by, or overlies, Winburn Granite.|Effusive and ignimbritic rocks; depositional layering; magma compositions are water-poor but F-, alkali- and FeO-rich, and reflect very high eruptive temperatures (>900 degrees C).|07-OCT-14
76740|Mount Palgrave Group|69153|5|Briefly described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen||Bentley Supergroup|Mount Waugh Formation, Scamp Formation, Eliza Formation||Felsic volcanic and volcaniclastic rocks, sandstone, siltstone and mudstone; minor mafic volcanic rocks|
76740|Mount Palgrave Group|69655|5|Briefly described|p3, p6, p26, p66|Stenian|Stenian|Musgrave Region.|c. 1090-1040 Ma|Bentley Supergroup|||Rhyolites.|
76740|Mount Palgrave Group|69729|5|Briefly described|p66 Fig.1, p68, p70, p80, p82, p85|||Stratigraphically lowest unit in the Talbot Sub-basin, Musgrave Province.||Bentley Supergroup.|Eliza and Scamp Formations, Mount Waugh rhyolite.|Is overlain by the Kaarnka and Pussy Cat Groups.|Aphyric to sparsely feldspar-phyric vitric rhyolites, with minor intercalations of basalt, basaltic andesite, siliciclastic conglomerates, and volcanogenic sandstones and mudstones.|
76740|Mount Palgrave Group|70095|5|Briefly described|p16-18|||Geological province: Musgrave Province. Of Talbot Sub-basin, Bentley Basin. Earliest preserved unit in the Talbot Sub-basin. Base of the section is not preserved; intruded by Winburn Granite. Comprises approximately 3.5km rhyolitic thickness and 0.1km basaltic thickness, over 200km strike length with multiple eruptive events.||Unit of Bentley Supergroup.|Includes Mount Waugh rhyolite, Scamp Formation and Eliza Formation.|Overlain by Pussy Cat Group/Kaarnka Group. Underlain by Winburn granite or Giles intrusions or Kunmarnara Group.||
76740|Mount Palgrave Group|70134|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Bentley Supergroup.|Scamp, Mount Waugh Formations.|Is overlain by Pussy Cat Group.||
76740|Mount Palgrave Group|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Bentley Supergroup.|Scamp, Mount Waugh Formations.||Rhyolite, basalt and interbedded siliciclastic rocks including diamictite, conglomerate, sandstone and siltstone.|
76740|Mount Palgrave Group|70634|6|Mentioned|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|SHRIMP ages from rhyolite (189580.1.pdf)|1063 Ma +/- 8 Ma||Includes Eliza Formation, Scamp Formation, Mount Waugh Formation|||
76740|Mount Palgrave Group|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Sample GSWA 189580 (rhyolite) yielded an interpreted (regression intersecting concoria curve) magmatic crystallisation age of 1063+\-8 Ma. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 2_5m_interpgeop15_lut.csv.|1077-1047 Ma (inferred)|Unit of Bentley Supergroup.|Includes Eliza Formation, Mount Waugh Formation, Scamp Formation.|Lowermost stratigraphic unit of Bentley Supergroup.|Felsic volcanic and volcaniclastic rocks, sandstone, siltstone, and mudstone; minor mafic volcanic rocks|
76740|Mount Palgrave Group|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Bentley Basin. ||Bentley Supergroup||||
76740|Mount Palgrave Group|70831|5|Briefly described|p3, p5, p9|Stenian|Stenian|Musgrave Province. Referred to as the Palgrave Group on p9.||Bentley Supergroup||||
76740|Mount Palgrave Group|71170|5|Briefly described|p5-p6|||Talbot Sub-basin. Emplaced during the Giles Event. Appears as Palgrave Group on p6 fig 3.||Bentley Supergroup||||
76740|Mount Palgrave Group|71210|6|Mentioned|p5|||Talbot Sub-basin.||||||
76740|Mount Palgrave Group|71211|5|Briefly described|p6 fig 1.3, p7 fig 1.4, p10|||Talbot Sub-basin. See also p11, p24 fig 2.1, p26, p27 fig 2.3, p61, p84 fig 3.1, p86, p87 fig 3.2, p135, p136 fig 4.1, p197, p215-p216, p219, p234, p271. ||Bentley Supergroup|Includes the Mount Waugh Formation, Scamp Formation and the Mount Eliza Formation|Overlain by the Kaarnka Group and the Cleghorne Formation. Conformably overlain by the Pussy Cat Group.|Dacitic to rhyolitic volcanic and pyroclastic rocks intercalated with minor basalts and sedimentary rocks.|
76740|Mount Palgrave Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone, ignimbrite|
76740|Mount Palgrave Group|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Sample GSWA 189589 (rhyolite) yielded a regression intersecting concordia curve at 1063+\-8 Ma, interpreted as magmatic crystallisation age. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv.||Unit of Bentley Supergroup.|Includes Eliza Formation, Mount Waugh Formation, Scamp Formation.||Felsic volcanic and volcaniclastic rocks, sandstone, siltstone, and mudstone; minor mafic volcanic rocks|
76740|Mount Palgrave Group|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Bentley Supergroup|Includes Mount Waugh Formation, Scamp Formation, Eliza Formation.||Felsic volcanic and volcaniclastic rocks, sandstone, siltstone, and mudstone; minor mafic volcanic rocks.|
76740|Mount Palgrave Group|72094|4|Described|p3 Fig 2, 4, 10, 13|Stenian|Mesoproterozoic|Talbot Sub-basin, Bentley Basin. Oldest unit of the Bentley Supergroup.  Intruded by Warakurna Supersuite intrusions with U-Pb 1071+/-5, 1063+/-8 and 1049+/-8 Ma zircon ages (Smithies et al., 2013b). See also Palgrave Group p12.||Unit of Bentley Supergroup.|Includes Scamp Formation. Probably includes Elisa Formation.|Underlain, and intruded by fine- to medium-grained intrusions of the Warakurna Supersuite.|Felsic volcanic and volcaniclastic rocks interlayered with sandstone, siltstone and mudstone, and minor mafic volcanic rocks.|
76740|Mount Palgrave Group|72443|4|Described|p737-741, p753, p756|||Talbot Sub-basin. Is the stratigraphically lowest preserved unit in the Talbot Sub-basin. Has a strike length in excess of 200km and a maximum thickness of 5km. Depositional layering dips shallowly south and west. Geochemistry and petrology are discussed.||Bentley Supergroup|Includes the Eliza Formation, Scamp Formation and the Mount Waugh Rhyolite.|Overlain by the Kaarnka and Pussy Cat groups.|Aphyric to sparsely feldspar phyric rhyolites, basalt and siliciclastic rocks rich in volcanic detritus overlain by non-welded ignimbrite, diamictite and autoclastic breccia.|
76740|Mount Palgrave Group|73437|6|Mentioned|p151|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Talbot Sub-basin.||Bentley Supergroup||||
33980|Mount Parker Formation|22547|6|Mentioned|p22|||See also Mount Parker Sandstone p21.||||||19-MAY-15
33980|Mount Parker Formation|22754|5|Briefly described|p5 Tb. 1|||Age: <c.1000Ma.  Geological Province: Osmond Basin. Shown as Mount Parker Sandstone in Table 3.||||||19-MAY-15
33980|Mount Parker Formation|24503|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Sandstone, pebbly sandstone, conglomerate, siltstone, mudstone and breccia.  Geological Province:  Osmond Basin.||||||
33980|Mount Parker Formation|63866|5|Briefly described|p130, p132, p137|||Osmond Basin.||||Unconformably overlies the Kimberley Group.|Sandstone, pebbly sandstone, conglomerat and siltstone.|
33980|Mount Parker Formation|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Sandstone, pebbly sandstone, conglomerate, siltstone, mudstone, and breccia.||||||15-DEC-08
33980|Mount Parker Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Osmond Basin|||Includes 2 unnamed members||Sandstone, pebbly sandstone, poorly sorted, oligomictic pebble to boulder conglomerate, siltstone, grey-green mudstone, and breccia.|03-AUG-15
33980|Mount Parker Formation|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv. |||||Sandstone, pebbly sandstone, conglomerate, siltstone, mudstone and breccia, poorly sorted oligomictic pebble to boulder conglomerate.|
33980|Mount Parker Formation|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Osmond Basin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|2500-1600 Ma (Inferred)||||Sandstone (at times thinly bedded), pebbly sandstone, conglomerate, grey-green mudstone, siltstone and breccia; poorly sorted, oligomictic pebble to boulder conglomerate, pebbly sandstone, and coarse-grained sandstone; quartz sandstone clasts.|
33980|Mount Parker Formation|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1797 Ma||||Sandstone, pebbly sandstone, conglomerate, siltstone, mudstone and breccia. Poorly sorted, oligomictic pebble to boulder conglomerate.|
33980|Mount Parker Formation|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Osmond Basin.||||||
33980|Mount Parker Formation|71267|4|Described|GEOL_LUT_CSV files|Neoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Osmond Basin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|1797-541 Ma (inferred)||||Sandstone, pebbly sandstone, conglomerate, siltstone, mudstone, and breccia, poorly sorted, oligomictic pebble to boulder conglomerate, pebbly sandstone, and coarse-grained sandstone; quartz sandstone clasts.|
33980|Mount Parker Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoproterozoic|Paleoproterozoic|Osmond Basin.|||||Sandstone, pebbly sandstone, conglomerate, siltstone, mudstone, and breccia.|
22439|Mount Peron Sandstone|43297|6|Mentioned|Fig.5 p9.|||of Cattamarra Group. Informal name.||||||
38804|Mount Pickering Dolerite|23930|5|Briefly described|p131|||Geological Province: Yilgarn Craton. Maximum thickness: 600m.||||||
38804|Mount Pickering Dolerite|60978|6|Mentioned|p60|||A sill at Darlot gold deposit area. Geological Province: Yilgarn Craton.||||||
38804|Mount Pickering Dolerite|71166|5|Briefly described|p33|||Hosts the Centenary gold mineralisation in the Darlot area. ||||||
36944|Mount Ragged Formation|23727|5|Briefly described|p4 Fig 1.|||Mount is Mt. in text.||||||
36944|Mount Ragged Formation|64161|6|Mentioned|p578 Fig.1, p583|Mesoproterozoic|Mesoproterozoic|Metasediments. Of Albany-Fraser Orogen||||||
36944|Mount Ragged Formation|64580|4|Described|map legend||Mesoproterozoic|Quartzite and minor pelite.||||||15-DEC-08
36944|Mount Ragged Formation|65487|4|Described|p2, 24, 51-52, 56-57, 59; Figs.1, 27-28|Mesoproterozoic|Mesoproterozoic|Protoliths deposited between Stage 1 and Stage II tectonism (ie c.1260-1215 Ma). Interpreted as cover rocks overlying the Nornalup Zone. Found NW of the Malcolm Gneiss. Upper greenschist-lower amphibolite facies quartzites, muscovite quartzites and sporadic pelites. 1321 Ma maximum depositional age. Buried and metamorphosed 1154 +/- 15 Ma (rutile growth: Clark et al., 2000).||||||
36944|Mount Ragged Formation|67268|6|Mentioned|p4, p9, p16, p19|Mesoproterozoic|Mesoproterozoic|Nornalup zone. Protolith was deposited in intracratonic basins. Deformed and metamorphosed at around c. 1154 +/- 15 Ma (Clark et al 2000). Written as Mount Ragged Group p20.||||||15-JUN-22
36944|Mount Ragged Formation|67380|5|Briefly described|p5-6|Mesoproterozoic|Mesoproterozoic|Sandstone-dominated sediments from uplift and erosion of the Recherche Supersuite. Age from detrital rutile.|c.1154 Ma max. deposition.|||||
36944|Mount Ragged Formation|67722|6|Mentioned|p5 fig 2.2, 2.3, p90, 97|||Nornalup Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen. Used interchangeably with Mount Ragged Metasediments, p1.||||||
36944|Mount Ragged Formation|68186|4|Described|p3 Fig.2, p8, p11, p26, p28, p30, p40-41|Mesoproterozoic|Mesoproterozoic|See also Plate 1A. Part of younger cover rocks of the Ragged Basin which covers the Arid Basin supracrustal rocks and Kepa Kurl Booya Province. Sediment sourced from Recherche Supersuite. Deposition in shallow intracratonic basins. <1321 +/- 24 Ma (maximum depositional age). Buried and metamorphosed (amphibolite facies) at 1154 +/- 15 Ma.|1260-1215 Ma.|||Unconformably overlies Recherche Supersuite.|Upper-greenschist to lower-amphibolite facies, massive grey mature quartzites, muscovite quartzites, psammitic schists; interbedded with sporadic thin layers of pelitic rocks.|
36944|Mount Ragged Formation|68654|6|Mentioned|p2 fig 1, p3|Mesoproterozoic|Mesoproterozoic|Ragged Basin, Albany-Fraser Orogen.|<1260 Ma|||||
36944|Mount Ragged Formation|69003|6|Mentioned|p28, p43|||Albany-Fraser Orogen. Contains sediment derived from the Recherche Supersuite.||||||
36944|Mount Ragged Formation|69140|6|Mentioned|p2|||Geological province: Albany-Fraser Orogen. Largely underformed to moderately deformed granitic rock.||||||
36944|Mount Ragged Formation|69152|5|Briefly described|500k_geologyp08_lut||Mesoproterozoic||||||Quartzite and minor pelite.|06-AUG-15
36944|Mount Ragged Formation|69252|4|Described|p1-107|Mesoproterozoic|Mesoproterozoic|Spaggiari et al. (2009) after Clarke et al. (1954). Has been referred to as Mount Ragged Beds (Lowry and Doepel, 1974), and Mount Ragged Schist (Myers, 1995). Ragged Basin. Nornalup Zone, Albany-Fraser Orogen. Forms the Russell Range. Named after Mount Ragged. Sourced from Recherche Supersuite granitic rocks. Underwent high-T metamorphism. Three sedimentary logs with descriptions; lithology described in great detail with illustrations and thin-sections. Structural geology, metamorphism, depositional environment detailed. Maximum deposition age and minimum (intrusion) age respectively.|1314 +/- 19 Ma - 1175 +/- 12 Ma.|||Is intruded by Esperance Supersuite and Beenong Dyke Suite.|Sequences of masssive grey quartzite and quartz-muscovite schist, with minor sporadic components of quartz-pebble conglomerate and pelitic schist.|
36944|Mount Ragged Formation|69595|5|Briefly described|p3 fig 1, p26, p27, p58.|||Albany-Fraser Orogen, eastern Nornalup Zone. Oldest age given is the maximum depositional age. |1321 +/- 24 Ma  - 1261 +/- 31 Ma (SHRIMP)||||Upper greenschist to lower-apmhibolite facies metasedimentary rocks dominated by pale grey, medium-grained, well-sorted, planar cross -bedded quartzite that is locally interbedded with well-sorted granular, quartz dominated gritstone.|
36944|Mount Ragged Formation|70023|3|Fully described|p166-173,177,179-180,182-186|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen. Also of Barren Basin. Autochthonous formation deposited in an intracratonic setting (distal fluvial environment; large fluvial system dominated by a shifting complexof sandy braided channels; shallow oxygenated environement) entirely comprising the Ragged Basin. See p170-171 for detailed sedimentology and lithofacies descriptions. Clean quartzitic content suggest erosion of a granitic source. Restricted to the eastern Nornalup Zone (southern- and eastern most Kepa Kurl Booya Province; Lowry and Doepel, 1974; Clark et al., 2000; Spaggiari et al., 2009). Metamorphosed to amphibolite facies at c. 1154 Ma during Stage II Albany-Fraser Orogeny. SHRIMP U-Pb detrital zircons constrain a maximum depositional age of 1314+\-19 Ma. Zircons of c.1320 Ma age are likely derived from Recherche Supersuite granites (Clark et al., 2000; Spaggiari et al., 2014a). Sparse zircons of c. 1490 Ma may have been derived from Mulgathing or Sleaford complexes, Gawler Craton. Also contains c. 1810-1320 Ma detritus, most of which appears to be derived locally from the reworked craton margin that forms the Albany-Fraser Orogen basement. Intruded by Scott Rock granite with monzogranite age at c. 1175 Ma, indicating miminum age of intrusion and deformation, and contraining minimum age of deposition. Sedimentary protoliths are described.|<1314+\-19 Ma and >1175 Ma.|||Underlain by basement rocks of the Nornalup Zone. Intruded by Scott Rock granite.|Massive pink or grey quartzite and quartz-muscovite aluminosilicate schist, with minor quartz-granule conglomerate and pelitic schist.|17-JUL-19
36944|Mount Ragged Formation|70084|6|Mentioned|p219|Ectasian|Ectasian|Geological province: Albany-Fraser Orogen, Yilgarn Craton. Of the Ragged Basin.||||||
36944|Mount Ragged Formation|70085|6|Mentioned|p234|||Albany-Fraser Orogen.||||||
36944|Mount Ragged Formation|70089|6|Mentioned|p262, 264|||Albany-Fraser Orogen.||||||
36944|Mount Ragged Formation|70090|5|Briefly described|p443-445,454|Ectasian|Ectasian|Geological province: Albany-Fraser Orogen, West Australian Craton. Of Ragged Basin. Exposed in the eastern Nornalup Zone. Deposited in a shallow intracratonic basin, fed by a large fluvial system dominated by a shifting complex of sandy braided channels (Waddell et al., 2015). Dominant U-Pb detrital zircon age component is between 1825 and 1750 Ma (Spaggiari et al., 2014c; Waddell et al., 2015).||||||
36944|Mount Ragged Formation|70153|5|Briefly described|500k_interpgeop14_lut.csv|Mesoproterozoic|Mesoproterozoic|Ragged Basin, Albany-Fraser Orogen.|1321 +/- 24 Ma (isotopic) - 1150 Ma (inferred).||||Psammitic schist and quartzite interbedded with thin layers of pelitic rocks.|
36944|Mount Ragged Formation|70182|6|Mentioned|p2-3, p9-10, p15, p34|||Albany-Fraser Orogen.||||||
36944|Mount Ragged Formation|70256|6|Mentioned|p3|||Albany-Fraser Orogen.||||||
36944|Mount Ragged Formation|70732|6|Mentioned|p285|||Geological province: Albany-Fraser Orogen.||||||
36944|Mount Ragged Formation|70735|6|Mentioned|p28|||Albany-Fraser Orogen.||||||
36944|Mount Ragged Formation|70802|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen. Of Ragged Basin. Reflects deposition in a shallow intracratonic basin (Clark et al., 2000), possibly fed by fluvial processes involving sand-bearing braided channels (Waddell, 2013). Events: Albany-Fraser Orogeny Stage II (1225-1140 Ma); Albany-Fraser Orogeny (1330-1140 Ma). Samples GSWA 194866 and 194874 (psammitic schists) yielded weighted mean 207Pb*/206Pb* date of 1331+\-14 Ma and 1340+\-16 Ma, interpreted as maximum depositional ages of the sandstone samples. Sample GSWA 194875 (psammitic schist) yielded weighted mean 207Pb*/206Pb* date of 1314+\-19 Ma, interpreted as maximum depositional age of the sandstone. See 500k_interpgeop14_lut.csv, 250k_pre_mesozoic_interpgeop_lut.csv.s|1321+\-24 Ma; 1150 Ma (inferred)||||Psammitic schist and quartzite interbedded with thin layers of pelitic rocks|
36944|Mount Ragged Formation|70813|6|Mentioned|p3|||Albany-Fraser Orogen.||||||
36944|Mount Ragged Formation|70826|6|Mentioned|p10|Mesoproterozoic|Mesoproterozoic|Deposited prior to 1225-1140 Ma (stage 2 of the Albany Fraser Orogen)||||||
36944|Mount Ragged Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||quartzite, conglomerate|
36944|Mount Ragged Formation|71270|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen, West Australian Craton. Of Ragged Basin. Events: Albany-Fraser Orogeny Stage II (1225 - 1140 Ma); Albany-Fraser Orogeny (1330 - 1140 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv.|1321+\-24 Ma; 1314+\-9 Ma; 1175+\-12 Ma||||Psammitic schist and quartzite interbedded with thin layers of pelitic rocks|
36944|Mount Ragged Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Ragged Basin, Albany-Fraser Orogen.|Max age, 1314+/-19 Ma, Min 1175+/-12 Ma.||||Psammitic schist and quartzite interbedded with thin layers of pelitic rocks.|
36944|Mount Ragged Formation|72059|6|Mentioned|p56|Mesoproterozoic|Mesoproterozoic|Geological province: Fraser Zone, Albany-Fraser Orogen.||||||
36944|Mount Ragged Formation|73084|6|Mentioned|p66|||Albany-Fraser Orogen.||||||
36944|Mount Ragged Formation|73480|6|Mentioned|p216-217|||Nornalup Zone, Arid Basin.||||||
36944|Mount Ragged Formation|73597|6|Mentioned|p1178|||Albany-Fraser Orogen.||||||
76819|Mount Rankin Granite|69559|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|See also geologyp_lut.csv, 500k_interpgeop_lut.csv..|2669 Ma||||Granite, undivided; typically deeply weathered.|
76819|Mount Rankin Granite|70156|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|2669+\-19 Ma (isotopic)||||Granite, undivided; typically deeply weathered|
76819|Mount Rankin Granite|70204|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton.|||||Granite, undivided; typically deeply weathered.|
76819|Mount Rankin Granite|70794|5|Briefly described|500k_interpgeop_lut.csv|Neoarchean|Neoarchean|Also 100k_interpgeop_lut.csv, 100k_geologyp_lut.csv.|2669+/-19 Ma||||Granite, undivided; typically deeply weathered.|
33909|Mount Regal dacite|22449|6|Mentioned|Table3 P27||Archean|Age of unit is 3260 Ma||||||07-NOV-08
27847|Mount Roe Basalt|22471|6|Mentioned|26 fig 30|Archean|Archean|Geol .province: Pilbara.||||||07-NOV-08
27847|Mount Roe Basalt|22475|5|Briefly described|p493, Fig.2|Archean|Archean|Base of Fortescue Group. See also p498, Figure 3, Table 1||||||07-NOV-08
27847|Mount Roe Basalt|22717|5|Briefly described|P9||Proterozoic|||||||
27847|Mount Roe Basalt|23045|6|Mentioned|291 fig 8|||||||||
27847|Mount Roe Basalt|23046|5|Briefly described|171|||||||||
27847|Mount Roe Basalt|23255|5|Briefly described|p50||Archean|Age: 2.77Ga. Of Fortescue Group. Mount is Mt in text.||||||07-NOV-08
27847|Mount Roe Basalt|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Fortescue Group.||||||
27847|Mount Roe Basalt|23416|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. In the Hamersley Basin.||||||07-NOV-08
27847|Mount Roe Basalt|23484|4|Described|p26|Archean|Archean|Age:c. 2770Ma. Of Fortescue Group. Geological Province: Pilbara Craton Maximum thickness: 200m.||||||07-NOV-08
27847|Mount Roe Basalt|23570|3|Fully described|p41|Archean|Archean|See also p237 App. 1. Of Fortescue Group. Age: 2763+/-13Ma, 2775+/-10Ma (U-Pb). Underlain by Bellary Formation. Max. thickness: 2440m. Geological Province: Hamersley Basin.||||||07-NOV-08
27847|Mount Roe Basalt|23575|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Underlain by Bellary Formation. Geological Province Hamersley Basin.||||||07-NOV-08
27847|Mount Roe Basalt|23583|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Overlain by Gregory Granitic Complex. Geological Province Hamersley Basin.||||||07-NOV-08
27847|Mount Roe Basalt|23585|3|Fully described|p14|Archean|Archean|Age: c.3303 Ma. Of Fortescue Group. Overlain by Bamboo Creek Member. Underlain by Warrawagine Granitoid Complex. Hamersley Basin. Max. thickness: 500 m.||||||07-NOV-08
27847|Mount Roe Basalt|23598|4|Described|p12|Archean|Archean|Of Fortescue Group. Overlain by Hardey Formation. Geological Province: Pilbara Craton.||||||07-NOV-08
27847|Mount Roe Basalt|23755|4|Described|p57|Archean|Archean|See also page 17 table 1. Of Fortescue Group.||||||07-NOV-08
27847|Mount Roe Basalt|23757|5|Briefly described|p9 Table 1|Archean|Archean|Age: c.2772 Ma (SHRIMP U-Pb).||||||07-NOV-08
27847|Mount Roe Basalt|23784|5|Briefly described|p4 Tb. 1|Archean|Archean|||||||07-NOV-08
27847|Mount Roe Basalt|23789|4|Described|p6 Tb. 1|Archean|Archean|Basal unit. Of Fortescue Group. Geological Province: Pilbara Craton.||||||07-NOV-08
27847|Mount Roe Basalt|23793|4|Described|p39|Archean|Archean|Of Fortescue Group. Geological Province: Hamersley Basin||||||07-NOV-08
27847|Mount Roe Basalt|23794|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Geological Province Hamersley Basin.||||||07-NOV-08
27847|Mount Roe Basalt|23813|5|Briefly described|p112|Archean|Archean|Mount is Mt. in text.  Age: 2772Ma.  Geological Province: Pilbara Craton.  See also p90 Tb. 1.||||||07-NOV-08
27847|Mount Roe Basalt|23936|4|Described|Tb.1|Archean|Archean|Age: c.2.76-2.69 Ga. Geological Province: Pilbara Craton. Of the Fortescue Group. Overlain by Hardy Sandstone.||||||07-NOV-08
27847|Mount Roe Basalt|24023|4|Described|p26|Archean|Archean|Of Fortescue Group.  Geological Province: Hamersley Basin.||||||07-NOV-08
27847|Mount Roe Basalt|24024|5|Briefly described|Map Legend|Archean|Archean|Of the Fortescue Group. Geological Province: Pilbara Craton||||||07-NOV-08
27847|Mount Roe Basalt|24025|5|Briefly described|p14|Archean|Archean|Of Fortescue Group.  Geological Province: Hamersley Basin.||||||07-NOV-08
27847|Mount Roe Basalt|24110|5|Briefly described|Plate 1|Archean|Archean|Of the Fortescue Group.  Geological Province: Hamersley Basin.||||||07-NOV-08
27847|Mount Roe Basalt|24160|6|Mentioned|p167 Fig.85.|Early Proterozoic|Early Proterozoic|Whim Creek area.|||||Mafic and intermediate lavas.|
27847|Mount Roe Basalt|24184|5|Briefly described|p709|Archean|Archean|Overlain by Hardey Formation. Geological Province: Pilbara Craton||||||07-NOV-08
27847|Mount Roe Basalt|24185|5|Briefly described|p745 Tb.4|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
27847|Mount Roe Basalt|24352|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group.  Massive vesicular and glomeroporphyritic basalt.  Age: c.2770Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
27847|Mount Roe Basalt|24353|4|Described|p5, p9 Fig.5, p11 Tb.2|Archean|Archean|Age: 2770-2760Ma. Of the Fortescue Group. Max Thickness: 200m. Geological Province: Hamersley Basin.||||||07-NOV-08
27847|Mount Roe Basalt|24391|4|Described|p8-4 Fig.2|Archean|Archean|Age: 2770 Ma. Of Fortescue Group. Flood basalt. Overlies Lizard Hills Formation. Overlain by Hardey Formation. Geological Province: Pilbara Block.||||||01-JUL-14
27847|Mount Roe Basalt|24410|6|Mentioned|p200 Fig. 138|Archean|Archean|||||||07-NOV-08
27847|Mount Roe Basalt|24531|5|Briefly described|p7|Archean|Archean|Of the Fortescue Group (Mount Bruce Supergroup).  Age: c.2772Ma.||||||07-NOV-08
27847|Mount Roe Basalt|24533|5|Briefly described|p9, 5 Table 2|Archean|Archean|Basal unit of the Fortescue Group. Composed largely of either massive, vesicular or glomero-porphyritic basalt. Age: 2763 +/- 13 and 2775 +/- 10Ma. Geological Province: Hamersley Basin.||||||07-NOV-08
27847|Mount Roe Basalt|24534|5|Briefly described|Map legend|Archean|Archean|Of Fortescue Group.  Massive, vesicular and glomeroporphyritic basalt.  Age: c.2770Ma.  Geological Province: Hamersley Basin.||||||07-NOV-08
27847|Mount Roe Basalt|24541|3|Fully described|p11 Tb.2, p48-50|Paleoproterozoic|Neoarchean|Of the Fortescue Group. Age: c. 2770 Ma. Maximum Thickness: 200m. Unconformably overlies the Cherratta Granitoid Complex, Dampier Complex, Regal Formation and Cleaverville Formation.||||||07-NOV-08
27847|Mount Roe Basalt|24543|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group (Mount Bruce Supergroup).  Age: c.2770Ma.  Massive and vesicular basalt; local volcaniclastic sandstone and basaltic agglomerate and tuff.||||||07-NOV-08
27847|Mount Roe Basalt|24544|4|Described|p57 Fig.43|Archean|Archean|Of Fortescue Group. Overlies Bellary Formation. Overlain by Hardey Formation. Age: c. 2783 Ma. Geological Province: Hamersley Basin.||||||07-NOV-08
27847|Mount Roe Basalt|24554|5|Briefly described|p5, p13|||Of the Fortescure Group. Geological Province: Hamersley Basin, Pilbara Craton.||||||
27847|Mount Roe Basalt|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Of the Forterscue Group. Basalt, locally glomeroporphyritic, agglomerate. Age: >/=2765Ma. See also p133.||||||07-FEB-11
27847|Mount Roe Basalt|30766|6|Mentioned|p15|||||||||
27847|Mount Roe Basalt|31307|6|Mentioned|p80|||||||||
27847|Mount Roe Basalt|31308|6|Mentioned|p71|||||||||
27847|Mount Roe Basalt|31310|6|Mentioned|Fig. 28|||||||||
27847|Mount Roe Basalt|31311|6|Mentioned|p62|||re age dates||||||
27847|Mount Roe Basalt|31819|6|Mentioned|p80|||||||||
27847|Mount Roe Basalt|35084|6|Mentioned|p279|||||||||
27847|Mount Roe Basalt|35218|6|Mentioned|p3|||||||||
27847|Mount Roe Basalt|35260|5|Briefly described|Table 1|||||||||
27847|Mount Roe Basalt|35269|6|Mentioned|Fig.5|||||||||
27847|Mount Roe Basalt|35523|6|Mentioned|p61|||||||||
27847|Mount Roe Basalt|35641|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27847|Mount Roe Basalt|36551|6|Mentioned|Table 23|||||||||
27847|Mount Roe Basalt|36882|4|Described|p125|||||||||
27847|Mount Roe Basalt|36902|6|Mentioned|p13|||||||||
27847|Mount Roe Basalt|37297|6|Mentioned|Fig.2|||||||||
27847|Mount Roe Basalt|37373|6|Mentioned|Tab 2.VII|||||||||
27847|Mount Roe Basalt|37460|3|Fully described|Table 3.I|||||||||
27847|Mount Roe Basalt|37564|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27847|Mount Roe Basalt|38242|6|Mentioned|p202|||||||||
27847|Mount Roe Basalt|39200|6|Mentioned|Fig.3|||||||||
27847|Mount Roe Basalt|39424|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27847|Mount Roe Basalt|39426|4|Described|p10|||||||||
27847|Mount Roe Basalt|39672|6|Mentioned|Fig.2|||||||||
27847|Mount Roe Basalt|39697|3|Fully described|p116|||See also p133.||||||16-JAN-07
27847|Mount Roe Basalt|39837|6|Mentioned|p257|||||||||
27847|Mount Roe Basalt|40369|3|Fully described|p8|||||||||
27847|Mount Roe Basalt|40904|6|Mentioned|p86|||||||||
27847|Mount Roe Basalt|40933|4|Described|p2|||||||||
27847|Mount Roe Basalt|41250|5|Briefly described|Table 1|||||||||
27847|Mount Roe Basalt|41252|6|Mentioned|Table 1|||||||||
27847|Mount Roe Basalt|41263|6|Mentioned|p58|||||||||
27847|Mount Roe Basalt|41357|6|Mentioned|p124|||||||||
27847|Mount Roe Basalt|41635|5|Briefly described|p29|||||||||
27847|Mount Roe Basalt|41669|3|Fully described|p21|||||||||
27847|Mount Roe Basalt|41843|5|Briefly described|p67|||||||||
27847|Mount Roe Basalt|41957|5|Briefly described|p67|||||||||
27847|Mount Roe Basalt|42148|6|Mentioned|Table 1 P687|||||||||
27847|Mount Roe Basalt|42231|6|Mentioned|p335|||||||||
27847|Mount Roe Basalt|42260|6|Mentioned|p115|||||||||
27847|Mount Roe Basalt|42352|6|Mentioned|p21|||||||||
27847|Mount Roe Basalt|42471|4|Described|p5|||||||||
27847|Mount Roe Basalt|42472|5|Briefly described|Map legend|||||||||23-DEC-09
27847|Mount Roe Basalt|42686|5|Briefly described|map legend|Archean||||||||07-NOV-08
27847|Mount Roe Basalt|42704|5|Briefly described|Plate 2E|Archean||Combined with Bellary Formation in map legend. Vesicular basalt and basaltic agglomerate, pelite, feldspathic sandstone and conglomerate, pillowed metabasalt, metatuff.||||||01-JUL-14
27847|Mount Roe Basalt|42707|5|Briefly described|map legend|Archean||||||||07-NOV-08
27847|Mount Roe Basalt|42744|4|Described|p3|||||||||
27847|Mount Roe Basalt|42785|5|Briefly described|p267|||see also Fig.3 p264.||||||16-JAN-07
27847|Mount Roe Basalt|43055|4|Described|p14, Table 4|||Of the Fortescue Group.||||||16-JAN-07
27847|Mount Roe Basalt|43056|5|Briefly described|Map Legend|||Of the Fortescue Group.||||||16-JAN-07
27847|Mount Roe Basalt|43119|4|Described|p5|||Of the Fortescue Group.||||||16-JAN-07
27847|Mount Roe Basalt|43262|5|Briefly described|Map Legend||Archean|of the Fortescue Group.||||||07-NOV-08
27847|Mount Roe Basalt|43290|4|Described|p4||Archean|Of the Fortescue Group.||||||07-NOV-08
27847|Mount Roe Basalt|43595|5|Briefly described|Table 2-29,p219|||||||||
27847|Mount Roe Basalt|43652|6|Mentioned|p390|||||||||
27847|Mount Roe Basalt|43698|6|Mentioned|p5|||||||||
27847|Mount Roe Basalt|43821|5|Briefly described|map legend|Archean|Archean|Of Fortescue Group.||||||07-NOV-08
27847|Mount Roe Basalt|43822|5|Briefly described|map legend|Archean|Archean|Age: Approx 2760 Ma. Of Fortescue Group.||||||07-NOV-08
27847|Mount Roe Basalt|44150|6|Mentioned|p132 Fig.2-131, p137|||||Fortescue Group||Overlies Whim Creek Group or Mount Negri Volcanics unconformably. Is overlain by Hardey Sandstone.||
27847|Mount Roe Basalt|44152|4|Described|p166, p176 Fig.2-154, p177-178|||Kriewaldt (1964). Type area is near Andover. Shows substantial thickness variations over short lateral distances.||Fortescue Group.||Correlated with Koongaling Volcanics.|Massive, well-jointed basalt flows; minor intercalated conglomerate, sandstone, arkose, siltstone; local pillows and hyaloclastites, tuff and agglomerate.|
27847|Mount Roe Basalt|44229|5|Briefly described|Map Legend|Archean|Archean|Part of the Fortescue Group.  Massive, porphyritic, vesicular and amygdaloidal basalt; some pillow basalt.||||||07-NOV-08
27847|Mount Roe Basalt|44443|6|Mentioned|map legend|Paleoproterozoic|Paleoproterozoic|Of Fortescue Group.||||||07-NOV-08
27847|Mount Roe Basalt|44477|5|Briefly described|p.7, Table 1||Proterozoic|SF/50-6.||||||
27847|Mount Roe Basalt|44478|14|Not recorded|map legend||Proterozoic|||||||
27847|Mount Roe Basalt|44501|4|Described|p.6,13,14,15,Tb4,map||Paleoproterozoic|(ref. to Kriewaldt 1964). Lower Proterozoic. (F/50-7). Defn on Tech.File SF/50-3.||||||07-NOV-08
27847|Mount Roe Basalt|44502|14|Not recorded|map legend||Proterozoic|||||||
27847|Mount Roe Basalt|44536|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
27847|Mount Roe Basalt|44837|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
27847|Mount Roe Basalt|46319|4|Described|p12|Proterozoic|Paleoproterozoic|Of Fortescue Group.  Maximum thickness: 300m.||||||07-NOV-08
27847|Mount Roe Basalt|50131|6|Mentioned|p6 Fig. 4, p2|||Of Fortescue Group. Geological Province: Pilbara Craton.||||||22-APR-09
27847|Mount Roe Basalt|50189|4|Described|p19-20|Archean|Archean|Formerly included in the Cooieena Basalt. Of the Fortescue Group. Unconformably overlies Chimingadgi Trondjhemite and parts of the Warrawoona and Gorge Creek Groups, and the Muccan and Warawagine Granitoid Complexes. Max. Thickness: ~700m.||||||07-NOV-08
27847|Mount Roe Basalt|50227|5|Briefly described|p442, p443 Fig. 1|Archean|Archean|Mount is Mt in text.||||||07-FEB-11
27847|Mount Roe Basalt|50287|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group (Mount Bruce Supergroup). Geological Province: Hamersley Basin. Massive and amygdaloidal basalt.||||||07-NOV-08
27847|Mount Roe Basalt|50300|5|Briefly described|Map Legend|Archean|Archean|Of the Fortescue Group.  Geological Province: Hamersley Basin. Age: c. 2770Ma.||||||07-NOV-08
27847|Mount Roe Basalt|50370|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group (Mount Bruce Supergroup). Geological Province: Hamersley Basin, Pilbara Craton. Age: c. 2770 Ma||||||07-NOV-08
27847|Mount Roe Basalt|50381|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group (Mount Bruce Supergroup). Geological Province: Hamersley Basin, Pilbara Craton. Age: c. 2770 Ma||||||07-NOV-08
27847|Mount Roe Basalt|50382|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Geological Province: Hamersley Basin, Pilbara Craton. Age: c. 2770 Ma||||||07-NOV-08
27847|Mount Roe Basalt|50427|6|Mentioned|p188 Fig.9|Archean|Archean|Of Fortescue Group.||||||07-NOV-08
27847|Mount Roe Basalt|50544|3|Fully described|p44, p15 Tb. 1|Archean|Archean|Basal unit of the Fortescue Group.  Unconformable on Warrawigine and Muccan Granitoid Complexes, Chimingadgi Trondhjemite (Mount Edgar Granitoid Complex), and on the Warrawoona and Gorge Creek Groups.  Age: c.2775-2763Ma.  Max. thickness: 700m.||||||07-NOV-08
27847|Mount Roe Basalt|50555|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group (Mount Bruce Supergroup).  Massive, porphyritic, vesicular and amygdaloidal basalt and basaltic andesite; some pillow basalt.  Overlain by Tumbiana Formation.  Geol. Province: Hamersley Basin.||||||07-NOV-08
27847|Mount Roe Basalt|60373|4|Described|p145 Tb. 1, p147 Fig. 2, p150 Tb. 2|Archean|Archean|Of Fortescue Group. Overlain by Hardey Formation. Age: 2772+/-2Ma, 2763+/-13 and 2775+/-2Ma (SHRIMP). Also on p152, p161 Fig. 6.||||||17-DEC-12
27847|Mount Roe Basalt|60429|4|Described|p19-20|||Of Fortescue Gp. Unconformably overlies Chimingadgi Trondhjemite, parts of Warrawoona and Gorge Creek Gps and Muccan and Warrawaginee Granitoid Complexes; overlain by Hardey Fm. Max. thickness: 700m. Massive basalt + basaltic andesite. Detailed lithology.||||||07-FEB-11
27847|Mount Roe Basalt|60635|6|Mentioned|p51 Fig. 2.2A|||||||||
27847|Mount Roe Basalt|60706|5|Briefly described|p625 Fig.3, p637 Fig.9|Archean|Archean|Of the Fortescue Group. Age: 2763+/-13 Ma and 2775+/-10 Ma (SHRIMP). Geological Province: Hamersley Basin. Mount is Mt in text of figure.||||||07-NOV-08
27847|Mount Roe Basalt|61252|5|Briefly described|p65|||Unconformably overlies Lalla Rookh Sandstone.||||||
27847|Mount Roe Basalt|61259|5|Briefly described|p403|Archean|Archean|Overlain by Hardey Formation. Age: 2763+/-13Ma and 2775+/-10Ma. Geological Province: Pilbara Craton. Mount is Mt in text.||||||07-NOV-08
27847|Mount Roe Basalt|61265|4|Described|p43, p46-47 Fig. 2|Archean|Archean|Of the Fortescue Group. Basalt and high-Mg basalt. Age: 2775-2756 Ma (Arndt et al. 1991). Geological Province: Pilbara Craton. See also p51 Tb.2||||||07-NOV-08
27847|Mount Roe Basalt|61266|4|Described|p58 Tb.1|Archean|Archean|Of the Fortescue Group. Age: 2765 Ma (Arndt et al., 1991). Basalt, locally glomeroporphyritic; agglomerate. Geological Province: Pilbara Craton.||||||07-NOV-08
27847|Mount Roe Basalt|61268|5|Briefly described|p81 Tb.1|||Of the Fortescue Group. Amygdaloidal basaltic flows and breccias, and basaltic volcaniclastic sandstone. See also p80 Fig.2.||||||
27847|Mount Roe Basalt|62129|3|Fully described|p6|Archaean|Archaean|Of Fortescue Group. Max thickness: 100m.  Geological Province: Hamersley Basin. Basalt flows interbedded with thin beds of basaltic breccia.||||||07-FEB-11
27847|Mount Roe Basalt|62130|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Age: c. 2765Ma. Geological Province: Hamersley Basin, Pilbara Craton. Metamorphosed amygaloidal basaltic flows and breccia.||||||23-MAR-09
27847|Mount Roe Basalt|62576|5|Briefly described|p618 Fig. 1, p619|Archean|Archean|Of the Fortescue Group. Age: 2775+/-10Ma. Geological province: Pilbara Craton (Marble Bar sub-basin). Mount may be Mt in text. See also p620 Fig. 3.||||||07-NOV-08
27847|Mount Roe Basalt|63142|5|Briefly described|p487 Fig. 2|||Of the Fortescue Group. Geological Province: Warrawoona Syncline.||||||
27847|Mount Roe Basalt|63367|5|Briefly described|p230, p231 Fig.1, p233 Fig.3 |Neoarchean|Neoarchean|Marble Bar sub-basin. Exposures show pahoehoe flowtops, ie subaerial.|2.78 Ga|Unit in Fortescue Group.|||Flood basalt sequence.|
27847|Mount Roe Basalt|63372|4|Described|Map Legend|Archean|Archean|Of the Fortescue Group. Geological Province: Hamersley Basin. Age: 2772Ma. Underlies: Hardey Formation. Massive, vesicular, and glomeroporphyritic basalt.||||||07-NOV-08
27847|Mount Roe Basalt|63417|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group (Mount Bruce Supergroup). Age: c.2772Ma. Geological Province: Fortescue Basin. Basaltic volcanic rocks; local volcaniclastic and siliciclastic rocks.||||||07-NOV-08
27847|Mount Roe Basalt|63420|5|Briefly described|Map legend|Archean|Archean|Of Fortescue Group (Mount Bruce Supergp). Overlies Lalla Rookh Sst in places, and Bellary Fm; overlain by Kylena F. Age: c.2775Ma. Geological Province: Marble Bar Sub-basin/Hamersley Basin. Basaltic volcanic rock; local volcaniclastic siliciclastic rocks.||||||07-NOV-08
27847|Mount Roe Basalt|64326|5|Briefly described|p71 Fig. 1, p72|Archean|Archean|Basal unit of Fortescue Gp. Stratigraphic detail describes Mount Roe Basalt as it presents in the Pear Creek Centrocline (northern Hamersley Basin) - where the Fortescue Group succession is different from elsewhere. Thickness: <3km. Underlies Hardey Fm.||||||07-FEB-11
27847|Mount Roe Basalt|64384|5|Briefly described|p29 Tb. 5, p37|Archean|Archean|Of the Fortescue Group. Overlies Bellary Formation. Geological province: northen Pilbara Craton and southern Hamersley Basin.||||||07-FEB-11
27847|Mount Roe Basalt|64580|4|Described|map legend||Neoarchean|Of Fortescue Group. Amygdaloidal basaltic flows and breccia; and basaltic volcaniclastic sandstone; metamorphosed.||||||15-DEC-08
27847|Mount Roe Basalt|64621|5|Briefly described|Map legend|Archean|Archean|Of Fortescue Group. Massive silicified basalt, porphyritic vesicular and amygdaloidal basalt; some pillow basalt; dolerite, pebble conglomerate, sandstone; occurs as clasts in Hardey Formation above. Further lithological detail included.||||||07-NOV-08
27847|Mount Roe Basalt|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Frotescue Group. Age: 2775-2763Ma. Geological Province: Pilbara Craton. Massive, porphyritic, vesicular, and amygdaloidal basalt; some pillow basalt; weakly metamorphosed.||||||01-JUL-14
27847|Mount Roe Basalt|64724|5|Briefly described|p42 Fig. 3|Neoarchean|Neoarchean|Basalt erupted during extension of the Hamersley Basin.||Of Fortescue Group.||Overlies Bellary Formation, overlain by Hardey Formation.||02-APR-12
27847|Mount Roe Basalt|64936|5|Briefly described|map legend|Archean|Archean|Of Fortescue Group, Mount Bruce Supergroup. Under Hardey Formation; over Bellary Formation. Doleritic basalt, minor pillow basalt. Age: c. 2775 Ma (geochronology: NT Arndt et al 1991). Geol. Prov: Hamersley Basin, Pilbara Craton.||||||13-JAN-12
27847|Mount Roe Basalt|65008|4|Described|p7, p8 Fig.5, p13-15, p21, p22, p24, p41|Neoarchean|Neoarchean|Hamersley Basin. U-Pb zircon SHRIMP age determined by Arndt et al. (1991), and Wingate (1999). The 3 facies are mapped separately. < 500m thick. Discontinuous thick-bedded shale units occur in upper parts.|2775 +/- 10 Ma|Of the Fortescue Group||Unconformably overlain by the Hardey Formation. Unconformably underlain by the Gorge Creek Group, Corboy Formation, and Warrawoona Groups.|Massive, porphyritic, vesicular, and amygdaloidal basalt; some pillow basalt; weakly metamorphosed.|
27847|Mount Roe Basalt|65724|5|Briefly described|map legend|Neoarchaean|Neoarchaean|Of Fortescue Group. Under Hardey Formation; unconformable over Euro Basalt. Basalt; pebble conglomerate, includes sandstone, siltstone and shale. Age: c. 2772 Ma (geochron MTD Wingate 1999). Geol. Prov: Hamersley Basin, Pilbara Craton.||||||
27847|Mount Roe Basalt|65726|5|Briefly described|Map legend|Archean|Archean|Hamersley Basin, Pilbara Craton.|c.2772 Ma (Arndt et al. 1991).|Of Fortescue Group.|||Massive, porphyritic, vesicular and amygdaloidal basalt, some pillow basalt; polymictic pebble conglomerate, includes sandstone, siltstone and shale.|
27847|Mount Roe Basalt|65727|5|Briefly described|Map legend|Neoarchean|Neoarchean|Fortescue Basin.|c.2772 Ma (Wingate 1999).|Of Fortescue Group.|||Basaltic volcanic rocks, local volcaniclastic and siliciclastic rocks; polymictic, poorly sorted pebble conglomerate, locally includes sandstone, wacke, siltstone and shale.|
27847|Mount Roe Basalt|65825|4|Described|p7 Fig.4,  pp20-21. |Archean|Archean|Volcanic succession up to 2.5 km thick. Composition of the basal conglomerate is directly related to the basement rocks nearby.  |c.2.78 Ga (Arndt et al. 1991).|Unit in Fortescue Group.||Unconformably overlies Yilgalong Granitic Complex and Mosquito Creek Formation.|Subaerial basaltic lavas, aphyric, dark green-grey to blue-grey, sparse vesicles; volcaniclastic rocks; minor subaqueous basaltic lavas; local gabbro; rare epiclastic sedimentary rocks; basal sandstone and polymictic conglomerate.|
27847|Mount Roe Basalt|65827|3|Fully described|p12 Tb.3, p14 Tb.4, p32-34, p36|Neoarchean|Neoarchean|Basal unit of Fortescue Group. Fissure eruptions aged 2775-2766 Ma. Faulted against Zulu Granodiorite; unconformably overlies Farrel Quartzite, Cleaverville and Wyman Formations, Mount Edgar Granitic Complex; unconformably underlies Hardey and Kylena Formations; shown as equivalent to part of Nullagine Supersequence. Fed by feeder dykes of Black Range Dolerite Suite. Massive, amygdaloidal, tholeiitic basalt, locally pillowed.||||||
27847|Mount Roe Basalt|65828|5|Briefly described|Map legend|Archean|Archean|||Unit in Fortescue Group.|||Massive and amygdaloidal basalt.|
27847|Mount Roe Basalt|65829|3|Fully described|p7 Fig.3, p8, p10, p15,  p26.|Neoarchean|Neoarchean|Basal fluvial deposits include polymictic pebble conglomerate, sandstone, grey siltstone, and shale. Basalts are locally carbonate altered, or intersected by numerous quartz or chalcedony veins. The high percentage of locally derived basalt clasts in the overlying Hardey Formation implies uplift and erosion of this unit. Hosts the unpromising Meentheena copper prospect, with mineralization occurring at contacts with a mafic dyke of the Round Hummock Dolerite Suite.|2775 +/- 10 Ma (Arndt et al. 1991).|Basal unit in Fortescue Group.||Overlies unconformably the Euro Basalt. Is faulted against the Kylena Formation. Is overlain unconformably by Hardey Formation.|Basal fluvial deposits; massive, porphyritic, vesicular and amygdaloidal subaerial basaltic lavas; local pillowed flows; dark grey to greenish-grey; locally plagioclase crystals form glomeroporphyritic texture ("Chinese writing stone").|
27847|Mount Roe Basalt|66108|5|Briefly described|Map legend|Neoarchean|Neoarchean|Unit in Fortescue Group. Age shown as 2775-2763 Ma. Basaltic volcanic rock; local volcaniclastic and siliciclastic rocks.||||||
27847|Mount Roe Basalt|66217|4|Described|p5, p6 Table 1, pp45-46, pp52-54.|Neoarchean|Neoarchean|Fortescue Basin, Pilbara Craton. Up to 2580 m thick.|2775 +/- 10 Ma (Arndt et al. 1991).|Unit in Fortescue Group.||Overlies Bellary Formation. Is overlain unconformably by the Hardey Formation.|Mainly subaerial basaltic lavas, subaqueous basaltic (pillow) lavas, and water-lain volcaniclastic rocks; minor non-volcanigenic conglomerate, sandstone and argillite.|
27847|Mount Roe Basalt|66664|6|Mentioned|p4, p5, p8, p9. |||||Unit in Fortescue Group.||||
27847|Mount Roe Basalt|66685|5|Briefly described|p217 Fig.2|Archean|Archean||2772 +/-2 Ma (zircon U-Pb, Blake et al., 2004).|Fortescue Group||Underlies the Hardey Formation.|Includes conglomerate, basalt and lapilli tuff.|
27847|Mount Roe Basalt|66887|5|Briefly described|p21 Fig.11|||Pilbara Craton. Mount Roe Basalt and Koongaling volcanics shown together with single age range in Fig.11. Shown as Mt Roe Basalt in figure 11.|~2780-2760 Ma.|Fortescue Group||||14-DEC-16
27847|Mount Roe Basalt|67025|5|Briefly described|p319 Fig.2. |Archean|Archean|||Basal unit in Fortescue Group.||Unconformably overlies Millindinna Complex. Is overlain conformably by Hardey Sandstone.||
27847|Mount Roe Basalt|67130|5|Briefly described|p3 fig 2, p24 fig 17, p45, p46 fig 44|Neoarchean|Neoarchean||2775 - 2763 Ma|Fortescue Group||Overlies Bellary Formation, overlain by Hardey Formation|Basalt, basaltic breccia, intermediate tuff, volcanic conglomerate, granite boulder volcanic conglomerate, sedimentary conglomerate|
27847|Mount Roe Basalt|67183|6|Mentioned|p645 Tb.1|Archean|Archean|Present in the Southern Pilbara.||Fortescue Group||||
27847|Mount Roe Basalt|67201|4|Described|p28-29, p31, p49-50|||In northern Pilbara Craton, Fortescue Basin. Thickness varies due to irregular paleosurface beneath: 50 m-2.5 km or absent. Unconformably overlies irregular paleosurface composed of Whundo Group, Cleaverville Formation, and Whim Creek Group.||Fortescue Group||Overlies Bellary Formation. Unconformably overlies Woodbrook Formation. Is unconformably overlain by Hardey Formation. Fed by Black Range Dolerite Suite dykes.|Pile of mostly subaerial basaltic flows, and minor lacustrine pillow lava and hyaloclastite. Vesicular or porphyritic basalt. Is a source rock for conglomerates in overlying Hardey Formation.|24-NOV-16
27847|Mount Roe Basalt|67202|5|Briefly described|p51-52|Archean|Archean|Fortescue Basin. c.2.4km thick.||Basal Fortescue Group.||Is overlain by Hardey Formation.||
27847|Mount Roe Basalt|67229|6|Mentioned|p3 Fig.2|||Kriewaldt and Ryan (1967). Pilbara region.||||||22-JUN-20
27847|Mount Roe Basalt|67269|5|Briefly described|p5|Paleoarchean|Paleoarchean|||Fortescue Group.|||Basalt.|
27847|Mount Roe Basalt|67270|5|Briefly described|p5, p12|Neoarchean|Neoarchean||c.2770 Ma.|Fortescue Group.||Unconformably overlies Apex Basalt.||
27847|Mount Roe Basalt|68035|5|Briefly described|p291, p292 Fig 6|Neoarchean|Neoarchean|Fortescue Basin. |2775-2763 Ma|Of Fortescue Group.||Overlies Bellary Formation.|Basalt.|
27847|Mount Roe Basalt|68056|6|Mentioned|p170-171|Archean|Archean|Pilbara Craton. Appears as Mt. Roe Formation on p171.||Fortescue Group.||||
27847|Mount Roe Basalt|68101|5|Briefly described|p6|||||||Overlain ?unconformably by Hardey Formation.|Basalt.|
27847|Mount Roe Basalt|68280|5|Briefly described|p5, p36, p42, p54|Neoarchean|Neoarchean||2775-2763 Ma|Fortescue Group||Overlain by Hardey Formation, overlies Black Range Dolerite Suite|Basalt.|17-JAN-23
27847|Mount Roe Basalt|68281|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.|2775-2763 Ma (Arndt et al. 1991).|Of the Fortescue Group.|||Massive, porphyritic, vesicular, and amygdaloidal basalt; pillow basalt; metamorphosed.|
27847|Mount Roe Basalt|68283|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Marble Bar Sub-basin, Fortescue Basin.|c. 2775 Ma (Arndt et al. 1991).||||Basaltic volcanic rock; local volcaniclastic and siliciclastic rocks.|
27847|Mount Roe Basalt|68574|6|Mentioned|p3, p5|||||||||
27847|Mount Roe Basalt|69012|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin. Four facies are mapped separately.|2775-2763 Ma (Arndt et al., 1991)|Of the Fortescue Group.|||Undivided basaltic rocks, local volcaniclastic and siliciclastic rocks. Komatiitic basalt; basaltic volcanic breccia and agglomerate; basaltic tuff and mafic wacke with thin shale interbeds; sandstone, pebbly sandstone and minor conglomerate.|29-APR-14
27847|Mount Roe Basalt|69015|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin. Mapped as 2 unnamed sub-units.|2775-2763 Ma (Blake, 2001)|Of the Fortescue Group.|||Massive, porphyritic, vesicular, and amygdaloidal basalt, some pillow basalt, metamorphosed; basaltic volcanic breccia and agglomerate, local accretionary lapilli.|05-MAY-14
27847|Mount Roe Basalt|69028|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin. Includes 2 unnamed units mapped separately: metamorphosed felsic volcanic rock; and metamorphosed quartzofeldspathic sandstone, conglomerate, mudstone and siltstone.||Of the Fortescue Group.|||Massive, porphyritic, vesicular and amygdaloidal basalt; some pillow basalt; metamorphosed.|06-MAY-14
27847|Mount Roe Basalt|69080|5|Briefly described|p687|Neoarchean|Neoarchean|||Unit in Fortescue Group.||Overlies Bellary Formation. Is overlain by Hardey Formation.||
27847|Mount Roe Basalt|69166|5|Briefly described|500k_geologyp08_lut.csv|Neoarchean|Neoarchean||||||Amygdaloidal basaltic flows and breccia, basaltic volcaniclastic sandstone, felsic volcanic rock, quartzofeldspathic sandstone, conglomerate, mudstone and siltstone; metamorphosed.|
27847|Mount Roe Basalt|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Fortescue Group|||Boulder and pebble conglomerate. Shale, siltstone, sandstone and wacke. Ferruginous siltstone, sandstone and pebbly sandstone. Dolerite, silicified basalt, massive, porphyritic, basalt. Basaltic tuff and volcanic breccia. Komatiitic basalt.|
27847|Mount Roe Basalt|69185|5|Briefly described|GEOL_LUT_CSV files||Neoarchean|Geological Province: Pilbara Craton. Of Northwest, Northeast, and South Pilbara Sub-basins, Hamersley Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 2770 Ma|Unit of Fortescue Group.|||Amygdaloidal basaltic flows and breccia; and basaltic volcaniclastic sandstone; metamorphosed; quartzofeldspathic sandstone; conglomerate; mudstone; and siltstone; metamorphosed.|
27847|Mount Roe Basalt|69299|3|Fully described|p1,4-7,9,11,14,20-21,map,Fig.4,Tb.1,Tb.2|Archean|Archean|Hamersley Basin, Pilbara Craton. Deposition in subaerial to shallow marine environment. Hickman (1983): three volcanic formations of Fortescue Group (Mount Roe Basalt, Kylena Basalt and Maddina Basalt) described as composed of basalt and andesite. Thickness on COOYA POOYA: 0-200 m, possibly 500 m in northeast (concealed). Regionally unconformably overlies Bookingarra Group. Is uncomformably overlain by other Fortescue Group constituents on COOYA POOYA. |c.2770 Ma (Arndt et al. 1991; Wingate 1999).|Of Fortescue Group.||Unconformably overlies Whundo Group in NW corner of COOYA POOYA; is conformably or disconformably overlain by Hardey Formation.|Massive, vesicular, and glomeroporphyritic basalt on COOYA POOYA.|01-JUL-14
27847|Mount Roe Basalt|69301|4|Described|p16-18, p23|||Pilbara Craton. Fortescue Basin. Marble Bar Sub-basin, Northeast Pilbara Sub-basin, Northwest Pilbara Sub-basin, South Pilbara Sub-basin, Sequence 1. Thickness: locally up to 2.5 km. Distribution is now restricted to paleovalleys that existed on an extensive 2.78 Ga peneplain.||Fortescue Group|||Dominantly volcanic; plateau basalts. Paleovalley environments included local deposition of fluviatile conglomerate and sandstone and deposition of shale and limestone (siliceous calcium carbonate) between units of pillow basalt.|
27847|Mount Roe Basalt|69563|5|Briefly described|p699||||c.2775-2766 Ma|Unit in Fortescue Group.||||
27847|Mount Roe Basalt|69569|6|Mentioned|p285 Fig.1|||East Pilbara Terrane.||Fortescue Group.||||
27847|Mount Roe Basalt|69590|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Of Northeast Pilbara Sub-basin and Marble Bar Sub-basin, Fortescue Basin. Events: Pilbara Craton breakup. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|2775-2772 Ma (isotopic, inferred)|Unit of Fortescue Group.|||Basaltic tuff, volcanic breccia and basaltic volcanic rocks; dolerite; komatiitic and pillow basalt; sandstone, siltstone; locally ferruginous, shale, conglomerate and phreatomagmatic boulder conglomerate.|
27847|Mount Roe Basalt|69792|6|Mentioned|p1096 Fig.1, p1097 Fig.2|Neoarchean|Neoarchean|Age within this unit [?near base] shown as 2775 Ma.||Unit in Fortescue Group.||||22-JUN-20
27847|Mount Roe Basalt|70775|5|Briefly described|p97||||c. 2775 Ma|Fortescue Group||Unconformably overlies the Louden Volcanics.||
27847|Mount Roe Basalt|70795|6|Mentioned|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean||2775-2772 Ma|Fortescue Group|||Basaltic volcanic and siliciclastic sedimentary rocks; metamorphosed.|
27847|Mount Roe Basalt|71042|6|Mentioned|p66 fig 2|Neoarchean|Neoarchean|||Of Fortescue Group.||||
27847|Mount Roe Basalt|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||basic volcanic rock, sandstone, limestone, dolerite|
27847|Mount Roe Basalt|71803|4|Described|p365-p368, p371, p374-p377, p379-p380|Neoarchean|Neoarchean|Pilbara Craton. Referred to as the Mount Roe Formation on p365 and p379. An additional age of 2763 +/- 13 Ma is also derived from Arndt et al, 1991.|2775 +/- 10 (Arndt et al, 1991)|Fortescue Group||Overlain by the Hardey Formation.|Basaltic sheet flows with local pillow lavas and volcaniclastic rocks and minor non-volcanogenic sediments.|
27847|Mount Roe Basalt|71808|5|Briefly described|p7, p47, p97, p104|||Pilbara Craton. Synvolcanic with the Black Range Dolerite Suite. Only recognised in the Bellary, Rocklea and Wyloo domes.||Fortescue Group|||Basalt and andesite and sandstone.|
27847|Mount Roe Basalt|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Marble Bar Sub-basin; Northeast Pilbara Sub-basin, Fortescue Basin.|Max age 2775+/-1- Ma, min 2772+/-2 Ma.|Fortescue Group, sequence 1|||Basaltic volcanic rock; local volcaniclastic and siliciclastic rocks.|
27847|Mount Roe Basalt|72712|6|Mentioned|p7 , p8, p10 Fig.6, p8.|Neoarchean|Neoarchean|Mount is spelt Mt. in diagram. This unit is mostly missing in the study area.|c. 2775 Ma to c. 2763 Ma.|Fortescue Group.||Overlies Bellary Formation and unconformably underlies Hardey Formation.|Includes basalt.|
27847|Mount Roe Basalt|72758|5|Briefly described|p5, p17 Tb.1, p19-21, p58.|||Incorporates the 'Paulsen Volcanics'  of Horwitz (1978). This unit is 1500m thick on the northeastern flank thinning to the south west. Schistose in southwestern half of the Wyloo Dome. Shown as including Hardey Sandstone in Table 1 p17, but this not supported by text p19, p21.||Fortescue Group||Underlies Mount Jope Volcanics and overlies Pilbara Supergroup and Metawandy Granite.|Vesicular or amygdaloidal metabasalt, basaltic agglomerate, felsic to intermediate ashfall/lapilli tuff in thin lenses, and small amounts of sedimentary rock. Includes feldspathic, lithic, quartzitic sandstones, conglomerate, rare mudstones.|
27847|Mount Roe Basalt|73538|6|Mentioned|p4|Neoarchean|Neoarchean|Ages of 2763 +/- 13 Ma and 2775 +/- 10 Ma were reported by Mole et al. (2018). [Written as Mt. Roe Basalt Formation].|2763 +/- 13 Ma, 2775 +/- 10 Ma|Fortescue Group||Underlain by Bellary Formation. Overlain by Hardey Formation.|Mafic volcanics.|
27847|Mount Roe Basalt|73598|6|Mentioned|p1209|||East Pilbara Terrane.||Fortescue Group.||||
38618|Mount Scholl Complex|23784|5|Briefly described|p12|Archean|Archean|||||||07-NOV-08
26057|Mount Scratch Siltstone|36293|2|Defined|p59|Proterozoic|Proterozoic|||||||
26057|Mount Scratch Siltstone|36872|3|Fully described|p73|||||||||
26057|Mount Scratch Siltstone|37460|6|Mentioned|p178|||||||||
26057|Mount Scratch Siltstone|40346|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26057|Mount Scratch Siltstone|40347|6|Mentioned|p16|||||||||
26057|Mount Scratch Siltstone|71781|5|Briefly described|p55, Plate 3|||||Of Yandanooka Group?||||
77535|Mount Shea Porphyry|66880|6|Mentioned|p7. |Archean|Archean||2658 +/- 3 Ma.|||||
77535|Mount Shea Porphyry|73391|6|Mentioned|p26||||2658 +/- 3 Ma.||||Porphyritic rhyolite.|
31685|Mount Sholl Intrusion|43822|5|Briefly described|map legend|Archean|Archean|Layered mafic intrusions approx. 2925 Ma. Of Pilbara Supergroup.||||||07-NOV-08
31685|Mount Sholl Intrusion|64174|5|Briefly described|Map legend|Archean|Archean|Part of the Radley Suite (Sisters Supersuite). Gabbro, leucogabbro, serpentinised peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed.||||||04-DEC-08
31685|Mount Sholl Intrusion|64580|4|Described|map legend||Mesoarchean|Of Radley Suite. Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed.||||||15-DEC-08
31685|Mount Sholl Intrusion|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological Province: West Pilbara Granite-Greenstone Terrane, Central Pilbara Tectonic Zone, and southwest Pilbara inlier, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 2925 Ma|Unit of Radley Suite.|||Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed|
31685|Mount Sholl Intrusion|70775|5|Briefly described|p79|||Contains Ni-Cu mineralization consisting of aggregates of pentlandite, pyrrhotite and chalcopyrite within a thin gabbroic marginal layer. |||||Gabbroic layer overlain by a thicker ultramafic layer of peridotite and pyroxenite.|
31685|Mount Sholl Intrusion|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Radley Suite|||Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed.|
80497|Mount Solitaire Sandstone|63866|6|Mentioned|p99|||Shown as Mt Solitaire Ssts in time space plot with a max deposition age within the 1850-1800 Ma range (~1820 Ma).||||||29-MAR-18
27207|Mount Sylvia Formation|22682|5|Briefly described|p29|||Newman sequence. Overlies Bee Gorge Member. Overlain by Mount McRae Shale||||||
27207|Mount Sylvia Formation|22689|6|Mentioned|Fig. 1 p138|||Of Hamersley Group.||||||
27207|Mount Sylvia Formation|22701|5|Briefly described|Fig2,p39|Neoarchean|Neoarchean|Hamersley Group, Hamersley Basin. Overlies Bee Gorge Member of Wittenoom Formation. Overlain by Mount McRae Shale.||||||07-NOV-08
27207|Mount Sylvia Formation|23045|5|Briefly described|289|||Parent Hamersley Group||||||
27207|Mount Sylvia Formation|23046|6|Mentioned|183|||||||||
27207|Mount Sylvia Formation|23126|5|Briefly described|p383 Fig.3|||||||||
27207|Mount Sylvia Formation|23127|5|Briefly described|p376|||||||||
27207|Mount Sylvia Formation|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Hamersley Group.||||||
27207|Mount Sylvia Formation|23536|5|Briefly described|Fig 2 p 429|||||||||
27207|Mount Sylvia Formation|23575|5|Briefly described|Map Legend|Proterozoic|Archean|Of Hamersley Group.||||||07-NOV-08
27207|Mount Sylvia Formation|23612|5|Briefly described|p840|Proterozoic|Archean|Age: ~2600-2480 Ma.||||||07-NOV-08
27207|Mount Sylvia Formation|23813|5|Briefly described|p90 Tb. 1|Archean|Archean|Sedimentary carbonates and clastics.  Age: c.2.603Ga; c.2.56Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.||||||07-NOV-08
27207|Mount Sylvia Formation|23890|5|Briefly described|p5 Fig.2|||Of Hamersley Group. Geological Province: Hamersley Basin.||||||
27207|Mount Sylvia Formation|23936|4|Described|Tb.1|Archean|Archean|Age: c.2.56 Ga. Geological Province: Pilbara Craton. Parent: Hamersley Group. Overlying Unit: McRae Shale. Underlying Unit: Wittenoom Formation. Mount is Mt in text.||||||07-NOV-08
27207|Mount Sylvia Formation|24041|6|Mentioned|p492|||Mount is Mt in text||||||
27207|Mount Sylvia Formation|24231|5|Briefly described|p186 Fig.2|||Of Hamersley Group. Geological Province: Hamersley Basin.||||||
27207|Mount Sylvia Formation|24426|5|Briefly described|p218 Fig.3|Paleoproterozoic|Archean|Of Hamersley Group. Overlain by Mount McRae Shale. Overlies Wittenoom Dolomite. Written Mt in text. Geological Province: Hamersley Province.||||||07-FEB-11
27207|Mount Sylvia Formation|24544|4|Described|p57 Fig.43|Archean|Archean|Of Hamersley Group. Overlies Wittenoom Formation. Overlain by Mount McRae Shale. Geological Province: Hamersley Basin.||||||07-NOV-08
27207|Mount Sylvia Formation|24573|5|Briefly described|p671 Fig.2|Proterozoic|Proterozoic|Of the Hamersley Group. Mount is spelt Mt. in text. Geological Province: Pilbara Craton||||||
27207|Mount Sylvia Formation|29595|6|Mentioned|Fig.2|||||||||
27207|Mount Sylvia Formation|29596|6|Mentioned|Fig.2|||||||||
27207|Mount Sylvia Formation|29629|6|Mentioned|Fig.2|||||||||
27207|Mount Sylvia Formation|30437|6|Mentioned|p98|||||||||
27207|Mount Sylvia Formation|31021|5|Briefly described|p893|||||||||
27207|Mount Sylvia Formation|31670|4|Described|p911|||||||||
27207|Mount Sylvia Formation|31671|5|Briefly described|p11|||||||||
27207|Mount Sylvia Formation|31828|6|Mentioned|p40|||Stratigraphic table||||||
27207|Mount Sylvia Formation|32326|6|Mentioned|p122|||Hamersley Gp.||||||
27207|Mount Sylvia Formation|32389|6|Mentioned|Fig.3|||||||||
27207|Mount Sylvia Formation|33538|6|Mentioned|Fig.2|||||||||
27207|Mount Sylvia Formation|33540|6|Mentioned|Fig.2|||||||||
27207|Mount Sylvia Formation|33542|6|Mentioned|p412|||||||||
27207|Mount Sylvia Formation|33544|2|Defined|p86|Precambrian|Precambrian|||||||
27207|Mount Sylvia Formation|33687|5|Briefly described|p917|||||||||
27207|Mount Sylvia Formation|34066|4|Described|p5|||L.Prot.||||||
27207|Mount Sylvia Formation|34135|5|Briefly described|Table 2|||Lower Proterozoic. P11.||||||
27207|Mount Sylvia Formation|35052|6|Mentioned|Fig.2|||||||||
27207|Mount Sylvia Formation|35260|5|Briefly described|Table.3|||||||||
27207|Mount Sylvia Formation|35299|5|Briefly described|p893|||||||||
27207|Mount Sylvia Formation|35976|6|Mentioned|Fig.39|||||||||
27207|Mount Sylvia Formation|36091|5|Briefly described|p572|||||||||
27207|Mount Sylvia Formation|36247|6|Mentioned|Fig.2|||||||||
27207|Mount Sylvia Formation|36551|6|Mentioned|Table 23|||||||||
27207|Mount Sylvia Formation|36642|6|Mentioned|Table 1|||||||||
27207|Mount Sylvia Formation|36882|4|Described|p134|||||||||
27207|Mount Sylvia Formation|37297|6|Mentioned|Fig.2|||||||||
27207|Mount Sylvia Formation|37460|6|Mentioned|Fig.3.4|||||||||
27207|Mount Sylvia Formation|37704|6|Mentioned|Fig.1|||||||||
27207|Mount Sylvia Formation|37708|6|Mentioned|p1930|||||||||
27207|Mount Sylvia Formation|38790|6|Mentioned|p164|||||||||
27207|Mount Sylvia Formation|39200|4|Described|p285|||||||||
27207|Mount Sylvia Formation|39697|5|Briefly described|p126|||||||||
27207|Mount Sylvia Formation|40369|6|Mentioned|Plate 1|||||||||
27207|Mount Sylvia Formation|40987|6|Mentioned|Fig.3|||||||||
27207|Mount Sylvia Formation|41622|6|Mentioned|Fig.2|||||||||
27207|Mount Sylvia Formation|41768|5|Briefly described|Table 1|||See also P28||||||
27207|Mount Sylvia Formation|42013|5|Briefly described|Map Legend|Archean||||||||07-NOV-08
27207|Mount Sylvia Formation|42112|5|Briefly described|p8|||||||||
27207|Mount Sylvia Formation|42148|6|Mentioned|Table 1 P687|||||||||
27207|Mount Sylvia Formation|42190|6|Mentioned|Fig.4 Map|||||||||
27207|Mount Sylvia Formation|42471|5|Briefly described|p7|||||||||
27207|Mount Sylvia Formation|42472|5|Briefly described|Map legend|||||||||
27207|Mount Sylvia Formation|42495|6|Mentioned|p36|||See also Mount Sylvia Shale.||||||
27207|Mount Sylvia Formation|42686|5|Briefly described|map legend|Proterozoic|Archean|||||||07-NOV-08
27207|Mount Sylvia Formation|42704|5|Briefly described|Plate 2E|Proterozoic|Archean|Of the Hamersely Group. Combined with Mount McRae Shale and Wittenoom Dolomite in this map legend.||||||07-NOV-08
27207|Mount Sylvia Formation|42743|5|Briefly described|map legend|Proterozoic|Archean|||||||07-NOV-08
27207|Mount Sylvia Formation|42744|4|Described|p5|||||||||
27207|Mount Sylvia Formation|43064|5|Briefly described|Fig.2,p70|||||||||
27207|Mount Sylvia Formation|43119|5|Briefly described|p9|||of Hamersley Group||||||
27207|Mount Sylvia Formation|43210|5|Briefly described|Table 1 p3,p4.||Paleoproterozoic|of Hamersley Group.||||||07-NOV-08
27207|Mount Sylvia Formation|43262|5|Briefly described|Map Legend||Archean|of Hamersley Group.||||||07-NOV-08
27207|Mount Sylvia Formation|43290|5|Briefly described|p6||Archean|of Hamersley Group.||||||07-NOV-08
27207|Mount Sylvia Formation|44152|5|Briefly described|p178, p179 Fig.2-155, p182|||The "shale" may not be terrigenous clay or mud; rather a variant iron-formation.||Hamersley Group.||Overlies Wittenoom Dolomite. Is overlain by Mount McRae Shale.|Minor BIF.|
27207|Mount Sylvia Formation|44477|4|Described|p.10, Table 1||Proterozoic|SF/50-6.||||||
27207|Mount Sylvia Formation|44478|14|Not recorded|map legend||Proterozoic|||||||
27207|Mount Sylvia Formation|44481|5|Briefly described|map legend||Paleoproterozoic|||||||07-NOV-08
27207|Mount Sylvia Formation|44501|4|Described|p.6,17, table 4, map||Paleoproterozoic|(ref. to MacLeod et al 1963). (F/50-7). Lower Proterozic.||||||07-NOV-08
27207|Mount Sylvia Formation|44502|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
27207|Mount Sylvia Formation|44503|2|Defined|p.14, Tb.2, map|||Roy Hill Sheet. (F50-12).||||||
27207|Mount Sylvia Formation|44504|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
27207|Mount Sylvia Formation|44692|2|Defined|p.7,12,13,25,Tb.1|||Overlain by Mt.McRae Shale; Includes 3 persistent beds of jaspilite with interbedded dolomitic shale. (F50-11).||||||31-JAN-08
27207|Mount Sylvia Formation|44729|5|Briefly described|map legend|Proterozoic||Of Hamersley Group||||||
27207|Mount Sylvia Formation|50227|6|Mentioned|p444|||Probably misspelt/abbreviated - see Mount Sylvia Shale Formation?  Mount is Mt. in text.||||||07-FEB-11
27207|Mount Sylvia Formation|60373|5|Briefly described|p145 Tb. 1|Archean|Archean|Of Hamersly Group. Overlian by Brockman Iron Formation, underlain by Mount Sylvia Formation.||||||
27207|Mount Sylvia Formation|60706|5|Briefly described|p623 Fig.2|||Of the Hamersley Group. Overlies the Wittenoom Formation. Geological Province: Hamersley Basin. Mount is Mt in text (p634).||||||12-APR-05
27207|Mount Sylvia Formation|61265|6|Mentioned|p46-47 Fig.2|||Geological Province: Pilbara Craton.||||||
27207|Mount Sylvia Formation|61268|5|Briefly described|p79, p81 Tb.1|||Of the Hamersley group. Mudstone, siltstone, chert, iron-formation, and dolomite.||||||
27207|Mount Sylvia Formation|61575|5|Briefly described|p760 Fig. 2|||Mount is Mt in text of figure.||||||
27207|Mount Sylvia Formation|61576|5|Briefly described|p774 Fig. 1|||Of the Hamersley Group. Geological Province: Hamersley Basin.||||||
27207|Mount Sylvia Formation|61847|6|Mentioned|p296 Fig. 3|||Mount is Mt in text.||||||
27207|Mount Sylvia Formation|62129|3|Fully described|p9-10, p18|Archaean|Archaean|Of Hamersley Group. Conformably overlies Wittenoom Formation. Thickness: 30m. Geological Province: Hamersley Basin. Dolomitic shales and three prominent BIFs.||||||07-FEB-11
27207|Mount Sylvia Formation|62130|5|Briefly described|Map Legend|Proterozoic|Archaean|Of Hamersley Group. Geological Province: Hamersley Basin, Pilbara Craton. Pelite, chert, and volcanic sandstone.||||||23-MAR-09
27207|Mount Sylvia Formation|63153|6|Mentioned|p1360, p1362 Fig.3, p1363 Fig.4. |||Shows tighter, almost convoluted, folding.||Unit in Hamersley Group.||Overlies Wittenoom Formation. Is overlain by Mount McRae Shale.||
27207|Mount Sylvia Formation|63372|4|Described|Map Legend|Archean|Archean|Of the Hamersley Group. Geological Province: Hamersley Basin. Mudstone, siltstone, chert, banded iron formation, and dolomite. Underlies: Brockman Iron Formation. Overlies: Wittenoom Formation.||||||07-NOV-08
27207|Mount Sylvia Formation|63432|5|Briefly described|p736 Fig. 2|Proterozoic|Proterozoic|Mount is Mt in text of figure.||||||07-FEB-11
27207|Mount Sylvia Formation|64384|5|Briefly described|p35 Tb. 6, p36|||Of Hamersley Gp. Geol.prov: Hamersley Basin.Comprises shale, dolomite + 3 BIF units; between central/top BIF bands is 21m thick-feldspathic sandstone at Mount Whaleback.Top BIF band is the distinctive Bruno's Band which can be traced throughout the basin.||||||07-FEB-11
27207|Mount Sylvia Formation|64580|4|Described|map legend|Paleoproterozoic|Neoarchean|Of Hamersley Group. Mudstone, siltstone, chert, banded iron-formation, and dolomite; metamorphosed.||||||09-DEC-08
27207|Mount Sylvia Formation|64724|4|Described|p43, p42 Fig. 3|Neoarchean|Neoarchean|Sediments of the Hamersley Basin.||Of Hamersley Group.||||02-APR-12
27207|Mount Sylvia Formation|65194|6|Mentioned|p15 Fig.2.3, p16 Fig.2.4, p102|Proterozoic|Proterozoic|Age: Early Proterozoic. Shale with beds of chert, dolomite and BIF.||||||
27207|Mount Sylvia Formation|65683|5|Briefly described|p801 Fig2|||Of Hamersley Group. Underlies Mount McRae Shale; overlies Wittenoom Formation.||||||08-MAR-12
27207|Mount Sylvia Formation|65757|5|Briefly described|p84 Fig.2|Siderian|Neoarchean|See also [misspelt] Sylvia Formation p81, p87 Fig.7. Shown with Mt McRae Formation as age: 2504+/-5 Ma. Written Mt in text.||||||
27207|Mount Sylvia Formation|67025|4|Described|pp318-320, p324, p326 Fig.7.|||||Unit in Hamersley Group.||Conformably overlies Wittenoom Dolomite. Is overlain conformably by Mount McRae Shale.|Includes BIF.|
27207|Mount Sylvia Formation|67056|6|Mentioned|p419 Fig.2, p423. |||||Unit in Hamersley Group.||Overlies Wittenoom Formation. Is overlain by Bruno's Band.||
27207|Mount Sylvia Formation|67130|5|Briefly described|p3 fig 2, p24 fig 17, p34 fig 29|||||Hamersley Group||Overlies Wittenoon Formation, Bee Gorge Member, overlain by Mount McRae Shale|Banded iron formation|
27207|Mount Sylvia Formation|67183|6|Mentioned|p645 Tb.1|Archean|Archean|Present in the Southern Pilbara.||Hamersley Group||||
27207|Mount Sylvia Formation|67201|4|Described|p34, p51-53|||Thickness: 30 m. Characterised by triplet BIF macrobands. Visible at base of Hamersley Range Escarpment, overlying Wittenoom Formation. Shown as Mt. Sylvia Fm.||Hamersley Group|informal Brunos Band|Overlies Wittenoom Formation, and is overlain by Mount McRae Shale.|Shale, dolomictic shale, and three thin BIF members.|24-NOV-16
27207|Mount Sylvia Formation|67721|5|Briefly described|p38 Fig.9|Neoarchean|Neoarchean|Approximately 30 m thick.|c. 2553 Ma|Of the Hamersley Group.||||
27207|Mount Sylvia Formation|67855|5|Briefly described|p226, 227||||||||Alternations of thin-bedded shale, siltstone, chert and baneded iron-elastica formation.|
27207|Mount Sylvia Formation|68035|5|Briefly described|p292 Fig 6|Neoarchean|Neoarchean|Hamersley Basin.||Of Hamersley Group.||Overlies Wittenoom Formation, overlain by Mount McRae Shale.|Banded iron formation.|
27207|Mount Sylvia Formation|68280|5|Briefly described|p5, p41, p54|Neoarchean|Neoarchean||2560-2500 Ma|Hamersley Group||Overlies Wittenoom Formation, overlain by Mount McRae Shale|Banded iron formation.|17-JAN-23
27207|Mount Sylvia Formation|69028|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Hamersley Basin. Mapped with Mount McRae Shale as a single unit.||Of the Hamersley Group.|||Mudstone, siltstone, chert, banded iron-formation and dolomite; metamorphosed.|06-MAY-14
27207|Mount Sylvia Formation|69080|6|Mentioned|p687|||||Unit in Hamersley Group.||Overlies Wittenoom Formation. Is overlain by Mount McRae Shale.||
27207|Mount Sylvia Formation|69185|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Neoarchean|Geological Province: Pilbara Craton. Of Northwest, Northeast, and South Pilbara Sub-basins, Hamersley Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.||Unit of Hamersley Group.|||Mudstone, siltstone, chert, banded iron-formation, and dolomite; metamorphosed|
27207|Mount Sylvia Formation|69538|5|Briefly described|p517 Fig.3, p525, p529 Fig.9, p530|Paleoproterozoic|Paleoproterozoic|See also p531 Fig.11, p532 Tb.3, p564 Fig.37, p574-575, p578 Fig.47, p583-585. Local basement in many detrital iron ore deposits.||Unit in Hamersley Group.||Is overlain by Mount McRae Shale.||
27207|Mount Sylvia Formation|69563|6|Mentioned|p691 Fig.1|||||Unit in Hamersley Group.||||
27207|Mount Sylvia Formation|69590|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Neoarchean|Geological province: Capricorn Orogen. Of Hamersley Basin; of Aphthalmia Fold Belt. Events: Paterson Orogeny; Miles orogeny; Edmundian Orogeny; Capricorn Orogeny; Ophthalmian Orogeny; South Pilbara subsidence.||Unit of Hamersley Group.|||Mudstone, siltstone, chert, banded iron-formation, and dolomite; metamorphosed|
27207|Mount Sylvia Formation|69739|6|Mentioned|p69|||Hamersley Basin.||||Overlies Wittenoom Formation. Is overlain by Mount McRae Shale.||
27207|Mount Sylvia Formation|69745|6|Mentioned|p272-273, 278-279, 281-282, 287, 290|||Crops out in the Mount Wall Fe deposit area, Hamersley Province.||Hamersley Group.||||
27207|Mount Sylvia Formation|70795|4|Described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|West Australian Craton, Hamersley Basin|2541-2501 Ma||||Mudstone, siltstone, chert, banded iron formation and metamorphosed dolomite.|17-SEP-18
27207|Mount Sylvia Formation|71042|5|Briefly described|p66 fig 2|Paleoproterozoic|Neoarchean|Oakover Basin.||Hamersley Group||||
27207|Mount Sylvia Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||shale, chert, banded iron formation|
27207|Mount Sylvia Formation|71808|4|Described|vii, p2, p6, p23, p26-p27, p45, p53|||Hamersley province. Interbeds of lithologically equivalent rocks to the Bee Gorge Member and the Mount McRae Shale consist of carbonate-bearing shale and mudstone with numerous thin bands of chert and turbiditic carbonate beds. Readily distinguishable  on airphotos.An excellent exposure occurs in a steep gully on the southeast face of Erics Point. Distinguishing characteristics are discussed. See also p72, p84-p85, p117, p132, p135, p149-p150, p184-p185, p223, p235.||Hamersley Group||Overlies the Bee Gorge Member.|Banded iron formation.|
27207|Mount Sylvia Formation|72034|6|Mentioned|500k_interpgeop16_lut|Neoarchean|Neoarchean|Hamersley Basin.  Shown as a combined informal unit with Mount Sylvia Formation||Hamersley Group, lower||||
27207|Mount Sylvia Formation|72493|5|Briefly described|p30|||Hamersley Basin.||Hamersley Group.||Overlies Wittenoom Formation. Is overlain by Mount McRae Shale.|BIF.|
27207|Mount Sylvia Formation|72712|5|Briefly described|p3, p10, p7 Fig.4, p9 Fig.5.|Paleoproterozoic|Neoarchean|See also p11 Fig.8, p54 Fig.35.|c. 2565 Ma.|Hamersley Group||Overlies Wittenoom Formation and underlies Mount McRae Shale.||
27207|Mount Sylvia Formation|72758|5|Briefly described|p15 Tb.1, p23-24, p33.|||Grouped together with Mount McRae Shale on the accompanying Wyloo map. 30 m thick on Wyloo mapsheet.  Uppermost BIF is called Bruno's Band||Hamersley Group||Conformably overlies Wittenoom Dolomite and conformably underlies Mount McRae Shale.|Three thin BIF units separated by mudstone with minor chert and dolomite.|
27207|Mount Sylvia Formation|73022|4|Described|p2-3, p4 Fig.3|||Siliciclastic and carbonate beds represent distal turbidites and hemi-pelagites deposited on a deep-water shelf floored by continental crust. Includes the Lower Chert and Middle Chert marker horizons of Fe-chert and minor shale. Some ferruginous chert beds contain greenalite nanoparticles, syneresis structures and shrinkage structures indicting a depositional origin from hydrothermal vent plumes.||Hamersley Group|Bruno's Band|Overlies the Wittenoom Formation and Bee Gorge Member, underlies the Mount McRae Shale|Fine-grained siliciclastic and carbonate beds comprising shale, minor Fe-chert and banded iron formation, intercalated with regional chert bands including laminated chert.|
27207|Mount Sylvia Formation|73290|6|Mentioned|p784|||Hamersley Province.||||||
27207|Mount Sylvia Formation|73538|6|Mentioned|p4|||[Written as Mt. Sylvia Formation].||Hamersley Group||Underlain by Bee Gorge Member of the Wittenoom Formation. Overlain by McRae Shale.|Iron formation.|
23838|Mount Troy Formation|22753|5|Briefly described|Fig.3 p585|Ordovician|Ordovician|Spelt Mt Troy Formation.||||||24-NOV-08
23838|Mount Troy Formation|24449|5|Briefly described|p745|Caradocian|Llandeilian|Of Carribuddy Group.  Geological Province: Canning Basin.  see also p471 Fig. 2.  Mount is Mt. in text of figure.||||||24-NOV-08
23838|Mount Troy Formation|40837|2|Defined|p274|Downtonian|Downtonian|||||||27-JAN-10
23838|Mount Troy Formation|42030|6|Mentioned|p746|||||||||
23838|Mount Troy Formation|43563|6|Mentioned|Fig.2,p5|||||||||
23838|Mount Troy Formation|43599|6|Mentioned|p250, Fig.3|||||||||
23838|Mount Troy Formation|43656|6|Mentioned|Fig.2,p8|Caradocian|Caradocian|||||||
23838|Mount Troy Formation|43746|6|Mentioned|Fig.2,p11|Caradocian|Caradocian|||||||
23838|Mount Troy Formation|43818|6|Mentioned|Fig.2.p39||Silurian|||||||
23838|Mount Troy Formation|44143|4|Described|p.440 Table 4-19|Middle Devonian|Early Devonian|Unit in Carribuddy Group. Up to 34m thick; dolomite, shale and siltstone; sabkha and supratidal marine. Type section between 701 & 716m in Edgar Range 1 (MOUNT ANDERSON: 18 deg 45' 26" S, 123 deg 35' 33" E). Rare spores and pollen.||||||
23838|Mount Troy Formation|61551|6|Mentioned|p351 Fig.2. |Late Ordovician|Late Ordovician|||||||
23838|Mount Troy Formation|64334|5|Briefly described|p39|Ordovician|Ordovician|Canning Basin; subsurface only. Caradoc.||Carribuddy Group.||Overlies Bongabinni Formation. Is overlain by Nibil Formation.|Dolostone.|
23838|Mount Troy Formation|64643|5|Briefly described|p3 Fig. 2|Upper Ordovician|Upper Ordovician|Of Carribuddy Group?||||||
23838|Mount Troy Formation|64982|5|Briefly described|p698.|Early Ordovician|Early Ordovician|Thickness to 35 m; laterally equivalent to Minjoo Salt.||Unit in Carribuddy Group.||Overlies Bongabinni Formation. Is overlain by Nibil Formation.|Dolomite, shale and siltstones.|
23838|Mount Troy Formation|65449|3|Fully described|p1, p6-8, p13, p19-21, p23, p31, p37-38|Late Ordovician|Late Ordovician|See also p40, p47-50, p56-57; Plates 2-3, 5, 8-10. Lehmann (1984), after Mount Troy; type section is between 716-701m in Edgar Range 1. No core was cut from the type section: the definition is based on wireline log data and cuttings alone. Typically expressed as an interval of slightly lower gamma ray values compared to surrounding units due to increased dolomite content. Previous errors in identifying this unit are discussed. Can be recognised locally. Age from inferred correlation with Minjoo Salt. Potential reservoir for Bongabinni Formation oil.||Carribuddy Group.||Conformably and gradationally overlies Bongabinni Formation. Approximate lateral equivalent of Minjoo Salt. Is overlain conformably and gradationally by Nibil Formation.|A thin unit of pale grey dolomite with interbedded red, brown, and grey mudstone; the ratio varies regionally.|
23838|Mount Troy Formation|69312|6|Mentioned|p19|Ordovician|Ordovician|Canning Basin. Shown only as Mt Troy.||||Overlies the Bongabinni Formation. Overlain by the Nibil Formation.||11-FEB-20
23838|Mount Troy Formation|69883|6|Mentioned|p4-p5|Caradoc|Caradoc|Canning Basin. Supersequences provided.||Carribuddy Group||Overlies the Bongabinni Formation. Overlain by the Nibil Formation. Laterally equivalent to the Minjoo Salt.||
23838|Mount Troy Formation|71171|6|Mentioned|p2|||Canning Basin.||||||
23838|Mount Troy Formation|72497|5|Briefly described|p3 Fig.2.|Katian|Sandbian|Shown as occuring in the Anketell Tabletop, Ryan Shelves, Willara and Kidson Sub-basins, the Jurgurra and Barbwire Terraces and Broome Platform. Age shown as Caradocian~= Gisbornian - Eastonian (Aust), Sandbian - Katian (ICS)||Carribuddy Group||Conformably overlies Bongabinni Formation and underlies Nibil Formation and is laterally equivalent to Minjoo Salt.||
23838|Mount Troy Formation|73344|6|Mentioned|p6|Sandbian|Sandbian|[Written as Mt Troy Fm]. Canning Basin, subsurface. Part of supersequence B1.||Carribuddy Group||Underlain by Bongabinni Formation. Overlain by Nibil Formation. Equivalent[?] to Minjoo Salt.||
75243|Mount Venn Igneous Complex|66116|5|Briefly described|Map legend|Archean|Archean|Burtville Terrane, Yilgarn Craton. Consists of three units: metamorphosed leucodolerite; metamorphosed layered gabbro; and metamorphosed gabbro with minor pyroxenite or quartz gabbro components.||||||
75243|Mount Venn Igneous Complex|66121|5|Briefly described|Map legend|Archean|Archean|Burtville Terrane, Yilgarn Craton. Consists of several units including metamorphosed leucodolerite with xenoliths of Palkapiti Formation; metamorphosed layered gabbro; and metamorphosed gabbro with minor pyroxenite or quartz gabbro components.||||||
75243|Mount Venn Igneous Complex|68107|4|Described|p608 Fig.4, p610, p616.|Neoarchean|Neoarchean|Mount Venn Greenstone Belt, Burtville Terrane. > 2km thick. Folded, faulted and truncated by shear zone.|ca. 2769-2666 Ma|||Intrudes the Palkapiti Formation.|Layered mafic intrusion, which ranges in composiiton from gabbro to dolerite, with minor pyroxenite.|
75243|Mount Venn Igneous Complex|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Merolia Domain, Burtville Terrane, Eastern Goldfields Superterrane, Yilgarn Craton|||Includes 7 unnamed subunits.|includes xenoliths of felsic volcanic and clastic sedimentary rocks of the Palkapiti Formation|Leucodolerite with xenoliths; medium- to coarse-grained mafic schist; gabbro; minor pyroxenite or quartz gabbro components; megacrystic leucogabbro; layered leucogabbro; layered gabbro; all metamorphosed.|06-AUG-15
75243|Mount Venn Igneous Complex|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|See also 100k_geologyp14_lut.csv.|2769 - 2666 Ma (inferred).||||Medium- to coarse-grained mafic schist, leucodolerite; metamorphosed. Gabbro, megacrystic leucogabbro, layered leucogabbro and layered gabbro; all metamorphosed.|
75243|Mount Venn Igneous Complex|71168|6|Mentioned|p10|Neoarchean|Neoarchean|Burtville Terrane, Yilgarn Craton.||||||
75243|Mount Venn Igneous Complex|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Burtville Terrane.|||||Layered intrusion of gabbro, leucogabbro, and leucodolerite; metamorphosed; locally schistose.|
68507|Mount Wangee Dacite|63441|2|Defined|p10 Tb. 2|Archean|Archean|Of the Orpheus Supersuite.  Intrudes Ruth Well, Regal and Cleaverville Formations. Age: 3021+/-3Ma. Geological province: Pilbara Craton.||||||07-FEB-11
68507|Mount Wangee Dacite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Orpheus Supersuite. Geological province: Pilbara Craton. Quartz feldspar porphyry, rhyolite and dacite; chiefly intrusive; metamorphosed.||||||08-DEC-08
68507|Mount Wangee Dacite|64580|4|Described|map legend||Mesoarchean|Of Orpheus Supersuite. Quartz-feldspar porphyritic rhyolite, and dacite;chiefly intrusive; metamophosed.||||||15-DEC-08
68507|Mount Wangee Dacite|67201|4|Described|p16-17 Fig.9|Archean|Archean|Pilbara Craton. In Roebourne-Karratha area.||Orpheus Supersuite|||Quartz-feldspar porphyry, rhyolite, and dacite; chiefly intrusive; metamorphosed.|
68507|Mount Wangee Dacite|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Orpheus Supersuite.|||Quartz-feldspar porphyritic rhyolite, and dacite; chiefly intrusive; metamophosed|
68507|Mount Wangee Dacite|70775|5|Briefly described|p15, p50|||Pilbara Craton. This unit is very similar to the Rea Dacite but forms sills and small stocks farther to the north between Mount Wangee and Cleaverville.||Orpheus Supersuite|||Quartz-feldspar porphyry, rhyolite and dacite, chiefly intrusive; metamorphosed gabbro and dolerite.|
76741|Mount Waugh Formation|69009|5|Briefly described|Map Legend|Stenian|Stenian|Bentley Basin.  Only shown on Interpreted Bedrock Geology diagram.|1077-1063 Ma|Of the Mount Palgrave Group.||||28-MAY-15
76741|Mount Waugh Formation|69153|5|Briefly described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen||Mount Palgrave Group|||Quartz-muscovite schist; rhyolite; interbeds of diamictite, conglomerate, sandstone, siltstone and amygdaloidal basalt|
76741|Mount Waugh Formation|70134|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin. The two facies are mapped separately.|1077-1063 Ma.|Mount Palgrave Group.||Overlies Scamp Formation (?conformably).|Amygdaloidal basalt, with quartz-filled amygdales locally 5mm in size; rhyolite, typically flow-banded and sparsely quartz- and feldspar-phyric, locally abundant fiamme.|
76741|Mount Waugh Formation|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. The three facies are mapped separately.|1077-1063 Ma.|Mount Palgrave Group.||Overlies Scamp Formation. Is overlain by Glyde Formation. Is intruded by Warakurna Supersuite.|Rhyolite, typically flow-banded and sparsely quartz- and feldspar-phyric, locally abundant fiamme; diamictite, conglomerate, sandstone and siltstone with interbedded basalt; amygdaloidal basalt with quartz-filled amygdales locally 5mm in size.|
76741|Mount Waugh Formation|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|SHRIMP age from file (195230.1.pdf)|1047 Ma - 1077 Ma (Inferred) 1065 Ma  (SHRIMP)|Mount Palgrave Group|||Amygdaloidal basalt, flow banded rhyolite, quartz-muscovite schist. Diamictite; sub-rounded to angular mafic and rare felsic volcanic clasts interbedded with conglomerate, sandstone, siltstone and amygdaloidal basalt.|
76741|Mount Waugh Formation|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Underwent peak metamorphic conditions at c. 1070 Ma (Howard et al., 2011). Samples GSWA 194794, 194795 and 194796 (mylonitic schists) yielded Ar-Ar plateau ages of 712+\-10 Ma, 718+\-6 Ma and 713+\-8 Ma respectively, indicating uplift and cooling during the Neoproterozoic Cryogenian period (850-635 Ma). Sample GSWA 195230 (rhyolite) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) magmatic crystallisation age of 1065+\-9 Ma. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 500k_interpgeop_lut.csv.|1077-1047 Ma (inferred)|Unit of Mount Palgrave Group.||Uppermost stratigraphic unit of Mount Palgrave Group. Underlain by Scamp Formation.|Amygdaloidal basalt, quartz-muscovite schist, rhyolite, diamictite, conglomerate, sandstone and siltstone interbedded with amygdaloidal basalt.|
76741|Mount Waugh Formation|71211|6|Mentioned|p216|||||Mount Palgrave Group||||
76741|Mount Waugh Formation|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. [Also referred to as Mount Waugh Rhyolite]. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Underwent peak metamorphic conditions at c. 1070 Ma (Howard et al., 2011). Samples GSWA 194794, 194795 and 194796 (muscovite in mylonitic schist) yielded Ar-Ar plateau ages of 712+\-10 Ma, 718+\-6 Ma and 713+\-8 Ma respectively, interpreted as time of cooling, and indicates uplift and cooling during the Neoproterozoic Cryogenian period. Sample GSWA 195230 (rhyolite) yielded a concordia age of 1065+\-9 Ma, interpreted as mean magmatic crystallisation age of the rhyolite. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|1077-1047 Ma (inferred)|Unit of Mount Palgrave Group.||Uppermost unit of Mount Palgrave Group. Underlain by Scamp Formation.|Amygdaloidal basalt, rhyolite; typically flow banded and sparsely quartz- and feldspar-phyric; qtz-ms schist; diamictite, conglomerate, sandstone, siltstone, interbedded with amygdaloidal basalt.|
76741|Mount Waugh Formation|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1065+/-9 Ma (crystallisation: U-Pb zircon).||||Feldspar-rhyolite.|
76741|Mount Waugh Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Mount Palgrave Group|||Flow-banded rhyolite, locally interlayered with siliciclastic diamictite, conglomerate, sandstone and siltstone, and amygdaloidal basalt.|
76741|Mount Waugh Formation|72443|6|Mentioned|p738, p742, p756|||Appears as Mount Waugh rhyolite on p738.|1061 +/- 11 Ma (SHRIMP U-Pb)|Mount Palgrave Group||||
31336|Mount Webb Suite|24197|4|Described|p33, p58|Paleoproterozoic|Paleoproterozoic|Comprises Mt Webb Granite, Pollock Hills Fm and Kintore Volcs. Fractionated granite, with extensive alteration effects incl: sodic-calcic, sericitic and hematite-K-feldspar in granite. Ages:1615Ma, ~1640Ma.Geol.P: west Arunta Block. Eg.of Hiltaba Assoc.||||||07-FEB-11
31336|Mount Webb Suite|50369|5|Briefly described|p1.2, 1.5, 21.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Age: ~1615Ma.||||||07-NOV-08
31336|Mount Webb Suite|64726|6|Mentioned|p83 Fig.2.|||||||||
31336|Mount Webb Suite|67323|5|Briefly described|p90|||Georgina Basin. Heat production for geothermal energy briefly discussed.|||||Granite.|
81605|Mount Webber Gabbro|72251|4|Described|p51,63-65,67-68|Paleoarchean|Paleoarchean|Geological province: Pilbara Craton. Nomenclature proposed by this study (Petersson et al., 2019) to encompass metamorphosed gabbroic, leucogabbroic and anorthositic rocks (with weighted mean c. 3.578 Ga Pb/Pb zircon ages) in the South Daltons region, in the western part of the Shaw Granitic Complex, and associated with the proposed 3.59-3.58 Ga Mount Webber magmatic event. Represents oldest igneous rock emplacement in the Pilbara Craton. Other U-Pb zircon ages include 3.59, 3.58, 3.44 Ga. Represents variably differentiated fragments of a layered mafic intrusion, with mantle-derived parental magmas. O isotope analysis indicates gabbro crystallisation in equilibrium with mantle oxygen. Gabbro and leucogabbro components are significant older than surrounding granodiorite components, suggesting that the Shaw Granitic Complex is part of the basement assemblage on which the Pilbara Supergroup is deposited on. Intrudes the South Dalton informal granodiorite.|3.59-3.58 Ga||||Metamorphosed gabbroic, leucogabbroic and anorthositic rocks.|11-FEB-20
34990|Mount Weld Carbonatite|23040|6|Mentioned|p151||Archean|Yilgarn Craton Province.||||||07-NOV-08
34990|Mount Weld Carbonatite|23337|6|Mentioned|898 Fig.3|||||||||
34990|Mount Weld Carbonatite|23573|5|Briefly described|p19|||||||||
34990|Mount Weld Carbonatite|24196|6|Mentioned|p11, p14 Fig.1|||Mount is Mt. in text.||||||
34990|Mount Weld Carbonatite|24494|6|Mentioned|p15|||See also Mount Weld carbonatite.||||||
34990|Mount Weld Carbonatite|50542|5|Briefly described|p140, p141 Fig. 104|Paleoproterozoic|Paleoproterozoic|Volcanic diatreme, 3km in diameter intruding Archaean greenstone. Geological Province: Yilgarn Craton.||||||07-FEB-11
34990|Mount Weld Carbonatite|64580|4|Described|map legend||Proterozoic|Carbonatite.||||||15-DEC-08
34990|Mount Weld Carbonatite|67127|6|Mentioned|p82, p126, p171|||Appears as Mount Weld Carbonatite Member on p171 (appendix).||||||
34990|Mount Weld Carbonatite|69152|5|Briefly described|500k_geologyp08_lut||Proterozoic||||||Carbonatite.|06-AUG-15
34990|Mount Weld Carbonatite|70153|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic||2020 +/- 17 Ma (isotopic).||||Carbonatite plug with mineralized lateritic cap; breccia with abundant glimmerite; locally silicified.|
34990|Mount Weld Carbonatite|70826|6|Mentioned|p9, p13|Paleoproterozoic|Paleoproterozoic||c. 2020 Ma|||||
34990|Mount Weld Carbonatite|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Events: Western Australian events (4000 - 0.01 Ma). See 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|2020+\-17 Ma||||Carbonatite plug with mineralized lateritic cap; breccia with abundant glimmerite; locally silicified|
34990|Mount Weld Carbonatite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic||2020+/-17 Ma.||||Carbonatite plug with mineralized lateritic cap; breccia with abundant glimmerite; locally silicified.|
78383|Mount White Group|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2690 - 2660 Ma (inferred).||Includes Maria Mine Formation, Halfway Well Basalt, Vivien Formation.|||
78383|Mount White Group|71212|5|Briefly described|intro p2, intro p3, p136|||Yilgarn Craton. Includes the informal Vivien metasediments, Maria metasediments and intervening, interlayered basalts and gabbros. |||Includes the Maria Mine Formation, Halfway Well Basalt and the Vivien Formation.|||
78383|Mount White Group|71270|5|Briefly described|100k_interpgeop_lut.csv|||Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton.|||Includes Halfway Well Basalt, Maria Mine Formation, Mosquito Well Conglomerate, Vivien Formation.|||
78383|Mount White Group|72095|6|Mentioned|p3 Fig 2, p5 Fig 3|||Eastern Goldfields, Yilgarn Craton.||||||
78383|Mount White Group|73151|4|Described|p2, p12, p14 Fig.9|Neoarchean|Neoarchean|Yilgarn Craton, Kalgoorlie Terrane, Agnew Greenstone Belt. Poorly exposed 1500-m-thick succession. 2686 +/- 7 Ma maximum depositional age from near the base of the sequence (Squire et al., 2010). Upper contact truncated by the Emu Shear Zone. Equivalent to the Vivien Sequence of Duuring et al., (2010)?|2686 +/- 7 Ma LA-ICPMS zircon||Vivien Formation, Halfway Well Basalt, Maria Mine Formation|Unconformably overlies east limb of Kalgoorlie Group.|Mostly sedimentary rocks. Predominantly polymictic conglomerate, fine- to coarse-grained sandstone and chert in lower part. Pillow basalt and gabbro as well as mudstone, sandstone and conglomerate in upper part.|
78383|Mount White Group|73596|6|Mentioned|p1152, 1156-1159, 1162|Neoarchean|Neoarchean|Agnew-Wiluna Greenstone Belt.|c.2690-2665 Ma.||Vivien, Maria Mine Formations; Halfway Well Basalt.|Overlies White Hope Basalt (Two Sisters Subgroup). Is overlain by Scotty Creek Formation.||
29295|Mount Wilson Sandstone|42710|5|Briefly described|map legend|Proterozoic||Variation on Mount Wilson Beds. Separated from main exposure by Devonian rocks. At least 666m thick.||Of Oscar Range Group||||17-OCT-12
29295|Mount Wilson Sandstone|42811|4|Described|p28|Neoproterozoic|Mesoproterozoic|of Oscar Range Group||||Unconformably overlain by Devonian rocks. Separated from Hooper Complex by shear zone.|Coarse-grained quartz sandstone, feldspathic sandstone and minor arkose.|17-OCT-12
29295|Mount Wilson Sandstone|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Oscar Range Group.|||Coarse quartz sandstone, feldspathic sandstone and minor arkose with abundant detrital tourmaline and zircon; generally less labile and finer grained upwards, with fine grained rippled micaceous sandstone near the top|
23841|Mowanjum Sand|36483|2|Defined|p67|Quaternary|Quaternary|Max. thickness: 15m. Geological Province: Canning Basin. Mainly of red to orange quartz sand; locally sand is white. Also, sheets and wedges of white sand, ferruginised sand and root-structured sand interlayered locally with the main red sand. Trace fossi||||||07-AUG-07
23841|Mowanjum Sand|37615|5|Briefly described|Table 1|||||||||
23841|Mowanjum Sand|64449|5|Briefly described|p63, p62 Tb. 2|Pleistocene|Pleistocene|Consists of structureless red sand (red sand and red muddy sand, root structures and mottled).||||||07-FEB-11
23841|Mowanjum Sand|73213|5|Briefly described|955, 956-957 Figs.1-2, 958-963, 965|Pleistocene|Pleistocene|Forms linear dunes. See also p967-968, 970.||||Unconformably overlies Broome Sandstone. Is overlain by Church Hill Sand, Cable Beach Sand, and locally Cape Gourdon Formation, Shoonta Hill Sand and/or Barn Hill Formation.|Red desert quartz sand. Shell middens occur on top of this unit.|
78890|Mu Formation|70793|4|Described|500k_interpgeop14_lut.csv|Cambrian|Cambrian|Of Amadeus Basin (Phase 1), Centralian Superbasin. Events: Areyonga Movement; Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma). See 500k_interpgeop14_lut.csv, 2_5m_interpgeop15_lut.csv.|541-485.4 Ma (inferred)||||Conglomerate, sandstone, mudstone|
78890|Mu Formation|70826|6|Mentioned|p2, p7 tbl 3|Cambrian|Cambrian|Amadeus Basin. ||||||
78890|Mu Formation|70839|5|Briefly described|p329-333,335,337-340,345|Cambrian|Cambrian|Of Amadeus Basin. Localised unit in the Mu Hills. Syn-tectonic origin, likely deposited during a late phase of the Petermann Orogeny accompanied by local salt movement. SHRIMP U-Pb zircon geochronology samples and analysis on p331-334. Two samples analysed, yielding maximum depositional ages of 631+\-15 Ma (238U/206Pb) and 833+\-9 Ma (238U/206Pb). See p332-333 for zircon age spectrums.||||Underlain unconformably by Maurice Formation.|Conglomerate and sandstone.|
78890|Mu Formation|71080|6|Mentioned|p29 fig 20|Cambrian|Ediacaran|Amadeus basin, WA.  Supersequence 4.||||||
78890|Mu Formation|71088|2|Defined|p1-p2, p7-p8, p12, p14, p16-p18|Cambrian|Cambrian|Amadeus Basin. Assigned to Supersequence 4; new name proposed by Peter Haines and Heidi Jane Allen (GSWA). Most outcrops now assigned to this unit were previously mapped as Ligertwood beds by Wells et al (1964; 1965). The type locality occurs on the northern edge of the Mu Hills  and outcrop is generally poor and discontinuous. Cobble and boulder conglomerates south of the Wallace Hills were previously assigned to the Sir Frederick Conglomerate but are now considered to overlie the Maurice Formation and are thus tentatively reassigned to the Mu Formation. This unit is at least 600m thick in the type area; however, the top of the unit is not exposed. Sample localities and descriptions are provided. Equivalent to the lower Pertaoorrta Group. Probably deformed in the Middle Ordovician. Outcrops at and near the type locality dip north around 20'. Deposited in an alluvial fan or fluvial environments. See also p20-p22, p24-p25, p33-p34.||||Unconformably overlies the Maurice Formation, Sir Frederick Conglomerate, Carnegie Formation and the Bitter Springs Formation.|Cobble and boulder conglomerate, sandstone interbedded with conglomeratic sandstone and minor silktstone.|03-MAY-23
78890|Mu Formation|71268|4|Described|GEOL_LUT_CSV files|Cambrian|Cambrian|Of Amadeus Basin (Phase 1), Centralian Superbasin. Events: Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma). See 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|541-485.4 Ma (inferred)||||Conglomerate, sandstone, mudstone|
78890|Mu Formation|71800|5|Briefly described|p26-p27|Early Cambrian|Early Cambrian|Amadeus Basin.||||Overlies the Maurice Formation. Unconformably overlain by the Chandler Limestone.|Sandstone breccia and medium sandstone.|
78890|Mu Formation|71810|5|Briefly described|Map legend.|Cambrian|Cambrian|Amadeus Basin (Phase 1), Centralian Superbasin.|||||Cobble to boulder conglomerate with predominantly sedimentary clasts and ferruginous, friable, sandy matrix; local red-brown sandstone and pebbly sandstone, and minor siltstone (inferred to have been deposited during the Petermann Orogeny).|
78890|Mu Formation|72034|5|Briefly described|500k_interpgeop16_lut|Cambrian|Cambrian|Amadeus Basin (Phase 1).|||||Conglomerate, sandstone, mudstone.|
78890|Mu Formation|72601|6|Mentioned|p3 Fig.2|Cambrian|Ediacaran|Amadeus Basin.||||Underlain, unconformably in part, by the Julie Formation. Equivalent to Carnegie Formation, Arumbera Sandstone and Winnall beds.||
78890|Mu Formation|73346|6|Mentioned|p4, p24-25|Cambrian|Cambrian|Amadeus Basin. Age probably Cambrian.||||||
26778|Mudjalla Sandstone Member|7433|5|Briefly described|p43.|Jurassic|Jurassic|||Unit in Wallal Sandstone.|||Sandstone, mudstone and conglomerate; fluvial.|
26778|Mudjalla Sandstone Member|22767|5|Briefly described|Table3 P14, P23|Late Jurassic|Early Jurassic|||||||
26778|Mudjalla Sandstone Member|22776|4|Described|Table.3|Late Jurassic|Early Jurassic|Parent: Wallal Sandstone, ? over max age.||||||
26778|Mudjalla Sandstone Member|36634|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|Early ? to Late Jurassic.||||||
26778|Mudjalla Sandstone Member|45158|4|Described|p16|||||||||
30728|Mueller Conglomerate|64580|6|Mentioned|map legend|||Frasnian and Famennian conglomerates associated with Devonian reef complexes.||||||15-DEC-08
30728|Mueller Conglomerate|66127|4|Described|p139, Plates 3, 7. |Famennian|Givetian|Of Hocking and Playford (1998c); name for an isolated conglomerate body east of the Margaret Embayment, previously shown as Elma Conglomerate (Tyler et al. 1998). Named after Mueller Ranges. Clasts derived from Kimberley Basin. c.100 m thick. Precise age not known.|||||Large cobble and boulder conglomerate overlying Proterozoic rocks; alluvial-fan deposit.|
30728|Mueller Conglomerate|69099|5|Briefly described|500k_geologyp08_lut.csv|Famennian|Frasnian|Frasnian and Famennian conglomerates associated with Devonian reef complexes|||||Conglomerate and sandstone.|03-AUG-15
30728|Mueller Conglomerate|69165|6|Mentioned|500k_geologyp08_lut.csv|Famennian|Frasnian|||||||
77219|Muggamurra Dolerite|66299|6|Mentioned|p6 Fig.3.|Mesoproterozoic|Mesoproterozoic||c.1200 Ma.|||||15-OCT-12
77219|Muggamurra Dolerite|66887|5|Briefly described|p5 Fig.4|Mesoproterozoic|Mesoproterozoic|Gascoyne Province.|~1210 Ma estimated from Fig.4.|||||
77219|Muggamurra Dolerite|66950|6|Mentioned|p9 Fig.8|Stenian|Ectasian||c. 1200 Ma|||||
77219|Muggamurra Dolerite|69080|6|Mentioned|p686 Fig.4|Ectasian|Ectasian||c.1210 Ma.|||||
77219|Muggamurra Dolerite|69596|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|Yilgarn Craton.||||||
77219|Muggamurra Dolerite|71869|6|Mentioned|p4|||||||||
77219|Muggamurra Dolerite|72389|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Marnda Moorn Large Igneous Province. Gabanintha 1:100k map sheet 2644.||Marnda Moorn Suite|||Dolerite and gabbroic dykes.|28-AUG-20
78994|Mugs Luck Basalt Member|69583|5|Briefly described|p49|Mesoarchean|Mesoarchean|Murchison Domain.||Murrouli Basalt.||||
78994|Mugs Luck Basalt Member|69584|5|Briefly described|p5 Fig.2|Mesoarchean|Mesoarchean|||Murrouli Basalt||Overlain by the Kantie Murdanna Volcanics Member|Komatiite and komatiitic basalt.|
78994|Mugs Luck Basalt Member|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Murrouli Basalt.||||
78994|Mugs Luck Basalt Member|70226|5|Briefly described|Map legend.|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Carton. 10 facies are mapped separately.||Yalgoo Formation|||Pyroxene spinifex-textured basalt flows and banded iron formation; minor interlayered sedimentary and volcaniclastic rocks; includes komatiite, peridotite, ultramafic and mafic schist; metamorphosed to serpentinite.|16-DEC-15
78994|Mugs Luck Basalt Member|70796|5|Briefly described|100k_geologyl_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, Yalgoo100_2241_stratig.pdf. Numerous additional lithologies are discussed.|ca 2800 to 2793 Ma (inferred)|Yalgoo Formation|||Basalt, sansdstone and lesser finely laminated siltstone, banded iron formation and minor banded chert, volcaniclastic sandstone to siltstone.|
78994|Mugs Luck Basalt Member|70830|5|Briefly described|p58|||Youanmi Terrane.||||||
78994|Mugs Luck Basalt Member|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeol_lut.|2800-2793 Ma (inferred)|Unit of Yalgoo Formation.|||Pillowed and spherulitic basalt, pyroxene spinifex-textured basalt, locally metamorphosed and schistose, interlayered with mafic schist (actinolite-tremolite-chlorite assemblages) and tremolite-chlorite-actinolite+\-talc schist; sheared|
79622|Muir Hills intrusion|68996|6|Mentioned|p51|Mesoproterozoic|Mesoproterozoic|See also map p50. WAROX data suggest that the Muir Hills intrusion (G1) dips to the north at approximately 75 degrees. Thickness of pluton unknown, but was set at 5 km in this model.||Giles Suite.||||
27210|Muiron Member|23726|5|Briefly described|p92|Quaternary|Pliocene|Of Exmouth Sandstone. Overlying unit Tulki Limestone. Underlying unit Milyering Member. Geological Province: Carnarvon Basin.||||||
27210|Muiron Member|33593|2|Defined|p113|Pleistocene|Pleistocene|Prob. Pleistocene. Type section location  described.||||||16-APR-18
27210|Muiron Member|37016|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
27210|Muiron Member|39427|4|Described|Table 1|||||||||
27210|Muiron Member|41271|4|Described|p194|||||||||
27210|Muiron Member|66125|5|Briefly described|p133 Fig.4|||Ningaloo Reef area; onshore. Occupies a terrace between Milyering and Muiron Scarps.||Exmouth Sandstone.||Overlies Pilgramunna Formation.|Coarse-grained littoral deposits overlain by medium-grained aeolian deposits.|
23843|Mulali Member|13194|6|Mentioned|p395 Tb. 4-16, p399 fig 4-63|Cambrian|Cambrian|Type Section: Hart Spring 15o19'S 128o39'E. 10-40m thick shoaling-upward cycles, probably flood-tidal deltas.||Skewthorpe Formation||Overlies Hart Spring Sandstone. Overlain by Galawa Member (conformably).|Upward-coarsening cycles of sandstone and shale; minor sandy or stromatolitic dolomite.|
23843|Mulali Member|40993|2|Defined|p1|Late Cambrian|Middle Cambrian|Middle to Late||||||
23843|Mulali Member|41864|4|Described|p38|||||||||
36958|Mulgandinnah Monzogranite|23416|5|Briefly described|Map Legend|Archean|Archean|Of Shaw Granitoid Complex, Pilbara Craton||||||07-NOV-08
36958|Mulgandinnah Monzogranite|23755|5|Briefly described|p70|||Age: 2934+/-2 Ma. See also p18 Table 2.||||||
36958|Mulgandinnah Monzogranite|23783|5|Briefly described|p115 Fig. 64|Archean|Archean|Age: 2930Ma.||||||07-NOV-08
36958|Mulgandinnah Monzogranite|24531|5|Briefly described|p29,  p8-9 Fig. 3|Archean|Archean|Of the Shaw Granitoid Complex.  Intrudes the Coondina and Bamboo Springs Monzogranites.||||||07-NOV-08
36958|Mulgandinnah Monzogranite|24532|5|Briefly described|Map legend|Archean|Archean|Of the Shaw Granitoid Complex.  Age: c.2928Ma.||||||07-NOV-08
36958|Mulgandinnah Monzogranite|50381|5|Briefly described|Map Legend|Archean|Archean|Of Shaw Granitoid Complex. Geological Province: Pilbara Craton. Age: 2928 Ma||||||07-NOV-08
36958|Mulgandinnah Monzogranite|50423|5|Briefly described|p215, Fig.1||Archean|Age: 2930 Ma.||||||07-NOV-08
36958|Mulgandinnah Monzogranite|50427|5|Briefly described|p187 Fig.8|Archean|Archean|Age: 2930 Ma. Of Shaw Granitoid Complex.||||||07-NOV-08
36958|Mulgandinnah Monzogranite|61252|6|Mentioned|p67 Tb.1|||Of the Shaw granitoid complex.||||||
36958|Mulgandinnah Monzogranite|62576|6|Mentioned|p620|Archean|Archean|Age: 2930Ma. ||||||07-NOV-08
36958|Mulgandinnah Monzogranite|63441|5|Briefly described|p11 Tb. 2|Archean|Archean|Of Sisters Supersuite. Supersedes Mulgandinnah Adamellite. Ages: 2928+/-2Ma, 2929+/-4Ma and 2928+/-5Ma. Ma. Geological province: Pilbara Craton.||||||07-FEB-11
36958|Mulgandinnah Monzogranite|64654|5|Briefly described|Map Legend|Archaean|Archaean|Of Sisters Supersuite. Age: c. 2928Ma and c. 2926Ma. Geological Province: Pilbara Craton. Fine- to medium-grained biotite monzogranite; weakly foliated.||||||17-NOV-08
36958|Mulgandinnah Monzogranite|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Sisters Supersuite. Age: c. 2928Ma. Geological Province: Pilbara Craton. Fine- to medium-grained biotite monzogranite; weakly foliated.||||||
36958|Mulgandinnah Monzogranite|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Unit in Sisters Supersuite. 2934-2919 Ma. Fine- to medium-grained, magnetite-bearing biotite monzogranite; weakly foliated.||||||
36958|Mulgandinnah Monzogranite|68282|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|c.2928 Ma (Zegers, 1996).|Of the Sisters Supersuite||Intrudes Callina Supersuite.|Fine- to medium-grained, weakly foliated, magnetite-bearing biotite monzogranite; schlieric leucocratic (meta-)monzogranite with augen after K-feldspar megacrysts; sheets of grey and K-feldspar-megacrystic monzogranite in tonalitic orthogneiss.|
36958|Mulgandinnah Monzogranite|69012|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|c. 2928 Ma|Of the Sisters Supersuite.|||Comprises fine- to medium-grained, magnetite-bearing biotite monzogranite; weakly foliated.|29-APR-14
36958|Mulgandinnah Monzogranite|69015|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|2934-2919 Ma (Zegers, 1996)|Of the Sisters Supersuite.|||Fine- to medium-grained, magnetite-bearing biotite monzogranite; weakly foliated.|02-MAY-14
36958|Mulgandinnah Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Sisters Supersuite|||Fine- to medium-grained biotite monzogranite; weakly foliated. Schlieric and locally migmatitic, leucocratic metamonzogranite and monzogranite with augen after K-feldspar megacrysts. Sheets of monzogranite and K-feldspar megacrystic monzogranite.|
36958|Mulgandinnah Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; North Pilbara Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.|2934-2919 Ma (inferred)|Unit of Sisters Supersuite.||Interleaved with Callina Supersuite.|Fine- to medium-grained, magnetite-bearing biotite monzogranite; weakly foliated; schlieric, and locally migmatitic, leucocratic metamonzogranite and monzogranite with augen after K-feldspar megacrysts.|
36958|Mulgandinnah Monzogranite|71137|6|Mentioned|p3-4|Archean|Archean|Pilbara.|2928 +/- 2 Ma (SHRIMP: van Kranendonk, 2010).|||Intrudes Lalla Rookh Formation.||
36958|Mulgandinnah Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
36958|Mulgandinnah Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||Max age 2934+/-2 Ma, min 2919+/-2 Ma|Sisters Supersuite|||Magnetite-bearing biotite monzogranite, fine to medium grained; weakly foliated.|
27510|Mulgine Granite|35726|6|Mentioned|p15|||See also P41||||||
27510|Mulgine Granite|40346|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
27510|Mulgine Granite|40347|5|Briefly described|p13|||||||||
27510|Mulgine Granite|71809|5|Briefly described|map legend|Archean|Archean|Yilgarn Craton, Youanmi Terrane||Of Rothsay Suite.|||Muscovite metamonzogranite, biotite metagranodiorite, and hornblende metatonalite phases: host to Mo-W mineralization; locally strongly deformed.|
27511|Mulkerins Granite|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27511|Mulkerins Granite|44366|14|Not recorded|p.10, Table 1||Proterozoic|Definition on Tech.File E/52-5.||||||
27511|Mulkerins Granite|44367|14|Not recorded|map legend|||(Reprinted 1971), part of Lamboo Complex.||||||
27511|Mulkerins Granite|44398|14|Not recorded|map legend||Proterozoic|||||||
27511|Mulkerins Granite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Paperbark Supersuite.|||White coarse and even grained leucocratic granite, syenogranite, monzogranite, tourmaline muscovite aplite and quartz feldspar pegmatite|
27511|Mulkerins Granite|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen, North Australian Craton.||Paperbark Supersuite.|||Coarse- to medium-grained, biotite syenogranite and monzogranite.|
34402|Mulla Bulla Formation|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
28827|Mullalyup pegmatite|39161|6|Mentioned|p49|||||||||
34081|Mullamullang Member|22613|5|Briefly described|p22|||||||||
34081|Mullamullang Member|22626|4|Described|438|Middle Miocene|Middle Miocene|Geol province: Eucla Basin. Parent Nullarbor Limestone. Age from foraminifera fauna.||||||14-SEP-18
34081|Mullamullang Member|44133|5|Briefly described|p180, 184|Miocene|Miocene|Geological Province: Eucla Basin. Of the Nullarbor Limestone. ||||||
34081|Mullamullang Member|62640|5|Briefly described|pp70-71, p72 Fig.6, p73. |Miocene|Miocene||c.20 Ma.|Unit in Nullarbor Limestone.||Of the Nullarbor Limestone|Nodular algal limestone.|
34081|Mullamullang Member|70397|4|Described|p2-5,7-8,11,14|Middle Miocene|Middle Miocene|Eucla Basin. Depositional environment: calm shelf, water depths 15-30m. Maximum thickness: 8m. Entirely comprises of the Rhodolith Facies.||Unit of Nullabor Limestone.||Basal unit of Nullabor Limestone. Overlain by/interbedded with Rawlinna member. Underlain by Wilson Bluff Limestone.|Rhodolith rudstone and floatstone with an articulated branching coralline algae, small benthic foraminifera and echinoderm-fragment grainstone and packstone matrix.|
34081|Mullamullang Member|70771|4|Described|p4, p31, p53-p58, p60-p61|||Eucla Platform, Eucla Basin. Attains a maximum thickness of 10m along the Hampton Range. It is interpreted to represent a transgressive rhodolith gravel deposit typical of those that form in the lower photic zone.||Nullarbor Limestone||Overlain by the Rawlinna Member.|Algal limestone with floatstone and rudstone textures.|
34081|Mullamullang Member|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||limestone rudstone|
34081|Mullamullang Member|71361|5|Briefly described|p34, p80, p119|||Paleoenvironment discussed in detail. See also p122, p127, p129, p142, p144, p146-p147, p152.|||||Rhodolith rudstones and floatstones with articulated coralline algae fossils and echinoderm fragment grainstone and packstone matrix.|
78967|Mulliberry Granite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||3010 - 2600 Ma (inferred).||||Foliated biotite monzogranite, granodiorite and microgranite dykes interleaved with greenstone; metamorphosed.|
78967|Mulliberry Granite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2683=2640 Ma (inferred)||||Foliated biotite monzogranite, granodiorite and microgranite dykes interleaved with greenstone; metamorphosed|
28111|Mullingarra Gneiss|23761|6|Mentioned|p4 Fig. 2|||||||||
28111|Mullingarra Gneiss|36293|6|Mentioned|p53|||See also Fig.51.||||||
28111|Mullingarra Gneiss|36879|4|Described|p107|||||||||
28111|Mullingarra Gneiss|37298|6|Mentioned|Fig.1|||||||||
28111|Mullingarra Gneiss|40346|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
28111|Mullingarra Gneiss|40347|4|Described|p12|||||||||
28111|Mullingarra Gneiss|43296|5|Briefly described|Map Legend||Proterozoic|||||||
28111|Mullingarra Gneiss|43495|6|Mentioned|3-5||Precambrian|||||||
28111|Mullingarra Gneiss|44138|5|Briefly described|p266||||||||Pelitic, semipelitic and quartzo-feldspathic gneiss with lenses of quartzite and amphibolite, with pegmatite veins.|
28111|Mullingarra Gneiss|44237|14|Not recorded|Fig.2||Precambrian|||||||
28111|Mullingarra Gneiss|64580|4|Described|map legend||Paleoproterozoic|Quartzo-feldspathic, semi-pelitic and pelitic gneiss; granoblastic texture common; minor pegmatitic and granitic segregations; includes lenses of quartzite and amphibolite.||||||15-DEC-08
28111|Mullingarra Gneiss|69182|6|Mentioned|Ch2 p3|||Perth Basin. ||||||
28111|Mullingarra Gneiss|70796|4|Described|2_5m_interpgeop15_lut.csv|Mesoproterozoic|Paleoproterozoic|Pinjarra Orogen, Mullingarra Inlier. See also 500k_interpgeop_lut.csv.|ca.  2180 1058 (inferred)||||Quartzofeldspathic, semipelitic and pelitic gneiss; granoblastic texture common; minor pegmatitic and granitic segregations; includes lenses of quartzite and amphibolite.|
28111|Mullingarra Gneiss|70826|6|Mentioned|p10|Mesoproterozoic|Mesoproterozoic|Pinjarra Orogen.||||||
28111|Mullingarra Gneiss|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||quartzite, pegmatite, gneiss, amphibolite|
28111|Mullingarra Gneiss|71269|5|Briefly described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Pinjarra Orogen. Events: Pinjarra Orogeny (1095-990 Ma).See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv.|1113-1058 Ma )inferred)||||Quartzofeldspathic, semi-pelitic and pelitic gneiss; granoblastic texture common; minor pegmatitic and granitic segregations; includes lenses of quartzite and amphibolite|
28111|Mullingarra Gneiss|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Pinjarra Orogen.|||||Quartzofeldspathic, semi-pelitic and pelitic gneiss; granoblastic texture common; minor pegmatitic and granitic segregations; includes lenses of quartzite and amphibolite.|
41377|Mullugunya Granodiorite|44229|5|Briefly described|Map legend|Archean|Archean|Part of the Mount Edgar Granitoid Complex.  Medium-grained, grey, biotite-hornblende granodiorite; weakly foliated.||||||07-NOV-08
41377|Mullugunya Granodiorite|50189|4|Described|p15, 22|Archean|Archean|Of the Mount Edgar Granitoid Complex. Weakly foliated, medium-grained, biotite and hornblende bearing granodioirte where biotite is commonly altered by chlorite. See also p6 Fig. 3||||||07-NOV-08
41377|Mullugunya Granodiorite|50544|4|Described|p30|Archean|Archean|Of the Mount Edgar Granitoid Complex. Formerly of the Munganbrina Suite of Collins (1983, 1993). Intrudes Apex Basalt and Duffer Formation, and possibly Euro Basalt.  Weakly foliated, medium-grained, biotite and hornblende-bearing granodiorite.||||||18-DEC-12
41377|Mullugunya Granodiorite|50555|5|Briefly described|Map legend|Archean|Archean|Of the Mount Edgar Graniotid Complex.  Medium-grained, grey  biotite-hornblende granodiorite.  Geological Province: Pilbara Craton.||||||07-NOV-08
41377|Mullugunya Granodiorite|60429|4|Described|p6 Fig. 3, p15|Archean|Archean|Of Mount Edgar Granitoid Cplx.Faulted against Chimingadgi Trondhjemite on MUCCAN; intruded by it on MOUNT EDGAR. Age: >3471+/-5Ma. Weakly foliated, medium-grained, biotite- + hornblende-bearing granodiorite where biotite is commonly altered to chlorite.||||||07-FEB-11
41377|Mullugunya Granodiorite|63417|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite.  Age: 3308Ma. Geological Province: Pilbara Craton. Biotite-hornblende granodiorite; medium-grained; weakly foliated; metamorphosed.||||||07-NOV-08
41377|Mullugunya Granodiorite|63441|5|Briefly described|p8 Tb. 2|Archean|Archean|Of Emu Pool Supersuite. Age: 3308+/-4Ma. Geological province: Pilbara Craton.||||||07-FEB-11
41377|Mullugunya Granodiorite|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||Of Mount Edgar Granitoid Complex.|||Biotite-hornblende granodiorite; medium-grained, grey, weakly foliated.|
41377|Mullugunya Granodiorite|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c.3308 Ma.|Of Emu Pool Supersuite.|||Biotite-hornblende granodiorite; medium-grained, weakly foliated, metamorphosed.|
41377|Mullugunya Granodiorite|65827|3|Fully described|p6 Tb.2, p13 Tb.4, p24, p25, p57|Paleoarchean|Paleoarchean|Of Emu Pool Supersuite. Of Mount Edgar Granitic Complex. 3308+/-4 Ma (SHRIMP U-Pb zircon; Love et al. 2006). Intruded by Bishop Creek Monzogranite, Zulu Granodiorite, Chimingadgi Trondhjemite (also faulted against); intrudes Coppin Gap Granodiorite, Apex Basalt. Weakly foliated, medium-grained biotite-hornblende granodiorite.||||||
41377|Mullugunya Granodiorite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Age derived from sample of massive biotite granodiorite (178099.1.pdf)|3308 +/- 4 Ma (SHRIMP)|Emu Pool Supersuite|||Biotite--hornblende granodiorite; medium grained, weakly foliated and metamorphosed.|
41377|Mullugunya Granodiorite|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA 178099 (biotite granodiorite) yielded an interpreted igneous crystallisation age of 3308+\-4 Ma for the monzogranite (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3308 Ma (isotopic)|Unit of Emu Pool Supersuite.|||Biotite-hornblende granodiorite; medium grained, weakly foliated and metamorphosed|
41377|Mullugunya Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite|
41377|Mullugunya Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||Max age 3308+/-4 Ma, min 3297+/-4 Ma.|Emu Pool Supersuite|||Biotite--hornblende granodiorite; medium grained; weakly foliated and metamorphosed.|
23847|Mulya Dolomite|37016|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
23847|Mulya Dolomite|38988|6|Mentioned|p14|||||||||
23847|Mulya Dolomite|39427|2|Defined|p4|Precambrian|Precambrian|||||||
23847|Mulya Dolomite|40088|6|Mentioned|p223|||||||||
23847|Mulya Dolomite|40900|6|Mentioned|p32|||||||||
23847|Mulya Dolomite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, crystalline dolostone/dolomite|
75924|Mumba Psammite|66110|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Moogie Metamorphics. Age shown as between 2240-2125 Ma. Quartzofeldspathic psammitic schist commonly with chloritoid; local minor pelitic schist and quartzite.||||||
75924|Mumba Psammite|66299|4|Described|p51, pp55-70, p167.|Paleoproterozoic|Paleoproterozoic|Formerly Mumba Pelite (Occhipinti and Sheppard 2001). Contains detrital zircons derived from Halfway Gneiss. Most lithologies were metamorphosed to high-grade during Glenburgh Orogeny.|c.2240-c.2125 Ma. |Unit in Moogie Metamorphics.||Unconformably overlies Halfway Gneiss. Is unconformably overlain by Mount James Subgroup. Intruded by thin dykes of Moorarie Supersuite.|Psammitic and pelitic schists; quartzite, locally interbedded with dolomitic marble.|
75924|Mumba Psammite|66579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Unit in Moogie Metamorphics.|||Quartzofeldspathic psammite schist commonly with chloritoid; local minor pelitic schist and quartzite.|
75924|Mumba Psammite|66887|4|Described|p6|Rhyacian|Rhyacian|Max age: youngest detrital zircons age indicates protoliths of parent (Moogie Metamorphics) were deposited after c. 2240 Ma (Johnson et al. 2010). Suggested min age of deposition is c. 2125 Ma (metamorphic zircons and monazites in Mumba Psammite. Johnson et al. 2010). Age distribution of detrital zircons indicate they were partly derived from underlying Halfway Gneiss.|min age deposition c. 2125 Ma; max age c. 2240 Ma|Moogie Metamorphics|||Psammitic schist.|15-DEC-16
75924|Mumba Psammite|67371|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, Gascoyne Province. Includes two un-named but separately-mapped members: a pelitic schist with chloritoid, locally with relict garnet porphyroblasts; and metamorphosed quartz sandstone, granule metaconglomerate and quartzite gneiss, locally micaceous.|2240 - 2125 Ma.|Unit in Moogie Metamorphics.|||Quartzofeldspathic psammitic schist commonly with chloritoid; local minor pelitic schist and quartzite.|
75924|Mumba Psammite|67373|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, Gascoyne Province. |2240 - 2125 Ma.|Unit in Moogie Metamorphics.|||Quartzofeldspathic psammitic schist, commonly with chloritoid; local minor pelitic schist and quartzite.|
75924|Mumba Psammite|67843|3|Fully described|Throughout the article.|Paleoproterozoic|Paleoproterozoic|Formerly Mumba Pelite (Occhipinti and Sheppard, 2001). Forms three subparallel SE-trending belts, each about 3-10 km wide with strike lengths exceeding 50 km. SHRIMP U-Pb zircon ages are detailed. Probably sourced from Halfway Gneiss. Metamorphosed between 2240 Ma and 2125 Ma.|2369 +/- 8 to 2240 +/- 8 Ma.|Unit in Moogie Metamorphics.||Unconformably overlies Halfway Gneiss. Is interleaved with Halfway Gneiss, Dalgaringa Supersuite, Moorarie and Durlacher Supersuites.|Discontinuous layers of pelitic schist and quartzite, and discrete packages of pelite and quartzite.|
75924|Mumba Psammite|68521|5|Briefly described|Map Legend||Siderian|2 minor facies are mapped separately.|< c.2300 Ma|Of the Moogie Metamorphics.|||Quartzofeldspathic psammitic schist commonly with chloritoid; minor quartzite gneiss, locally with relict cross-bedding; pelitic schist, commonly with chloritoid, locally with relict garnet porphyroblasts.|
75924|Mumba Psammite|68522|5|Briefly described|Map Legend|Rhyacian|Rhyacian|Gascoyne Province. |2240-2125 Ma|Of the Moogie Metamorphics.|||Quartzofeldspathic psammitic schist commonly with chloritoid, local minor pelitic schist and quartzite; pelitic schists commonly with chloritoid, locally with relict garnet porphyroblasts; meta quartz sandstone, granule metaconglomerate and gneiss.|
75924|Mumba Psammite|69011|5|Briefly described|Map Legend|Rhyacian|Rhyacian|Glenburgh Terrane, Gascoyne Province.||Of the Moogie Metamorphics.|||Comprises metamorphosed quartz sandstone, granule metaconglomerate, and quartzite gneiss, locally micaceous; minor psammitic schist; locally with relict cross-bedding.|
75924|Mumba Psammite|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Age derived from psammitic schist sample (184160.1.pdf) and constrains the maximum age for deposition of sandstone protolith.|2485 Ma +/- 3 Ma  (SHRIMP)|Moogie Metamorphics|||Pelitic schist commonly with chloritoid; locally with relict garnet porphyroblasts. Metaquartz sandstone, granule metaconglomerate, quartzite gneiss, locally micaceous; minor psammitic schist. Quartzofeldspathic psammitic schist.|
75924|Mumba Psammite|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 183275.1.pdf  West Australian Craton, Bryah Basin|2240-2125 Ma|Moogie Metamorphics|||Quartzofeldspathic psammitic schist, commonly with chloritoid pelitic schist and quartzite. Metamorphosed quartz sandstone, granule metaconglomerate and quartzite gneiss, locally micaceous|
75924|Mumba Psammite|72259|6|Mentioned|p4|||[Article examines the age and geochemistry of rutile from this unit].|||||Includes quartzite.|
36943|Mummawarrawarra Basalt|23716|6|Mentioned|p11|||||||||
36943|Mummawarrawarra Basalt|24301|5|Briefly described|p13|Mesoproterozoic|Mesoproterozoic|Of Tollu Group.  Age: 1078+/-5Ma (Glickson et al, 1996). Geological Province: Musgrave Block.||||||05-AUG-08
36943|Mummawarrawarra Basalt|44109|4|Described|p9, p117|||Of the Tollu Group. Thick sequence of amygdaloidal mafic to intermediate flows and minor pyroclastic rocks. Max. thickness: 240m.||||||09-MAY-13
36943|Mummawarrawarra Basalt|61154|5|Briefly described|p17, p18 Fig. 10|Mesoproterozoic|Mesoproterozoic|Of the Tollu Group (Bentley Supergroup).  Amygdaloidal mafic to intermediate flows and minor pyroclastic rocks. Geological Province: Musgrave Block.||||||
36943|Mummawarrawarra Basalt|61339|5|Briefly described|Map legend|||Of the Bentley Supergroup.  Amygdaloidal basalts and tuff.||||||
36943|Mummawarrawarra Basalt|62989|6|Mentioned|p39|||Of the Tollu Group. Geochemically similar to Mount Harris Basalt.||||||25-JAN-07
36943|Mummawarrawarra Basalt|63864|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Tollu Group. Underlain conformably by Macdougall Formation and conformably overlain by Smoke Hill Volcanics. Consists of vesicular and amygdaloigal basalt and andesites; locally plagioclase porphyritic; epidotized.||||||15-JUL-08
36943|Mummawarrawarra Basalt|65135|4|Described|p16|Stenian||Amygdaloidal basalts. Overlies MacDougall Formation. Unconformably overlain by Smoke Hill Volcanics. Xenoliths of Mummawarrawarra Basalt included in Jameson and Blackstone intrusions. Mainly restricted to outcrops south of the poorly exposed southern limb of a syncline south of the Blackstone intrusion. Older than 1078 Ma.||||||
36943|Mummawarrawarra Basalt|65256|5|Briefly described|p14, p16|||Of the Tollu Group. Conformably overlies MacDougall Formation; overlain by Smoke Hill Felsic Volcanics; correlative of Mount Harris Basalt (Tjauwata Group). Amygdaloidal mafic to intermediate flows and minor pyroclastic rocks; locally intruded by basaltic dykes and gabbroic stocks. ||||||
36943|Mummawarrawarra Basalt|65693|6|Mentioned|p3.|||||||Intruded by Bell Rock and Blackstone intrusions.||
36943|Mummawarrawarra Basalt|65833|4|Described|p16|Stenian|Stenian|Of Kunmarnara Group (Smithies et al., 2008); formerly of Tollu Group (Daniels, 1971). Overlies MacDougall Formation; overlain by Smoke Hill Volcanics. Amygdaloidal basalts. Age >~1078 Ma.||||||
36943|Mummawarrawarra Basalt|65906|6|Mentioned|p6, p20|Mesoproterozoic|Mesoproterozoic|Unit in Bentley Supergroup. Correlative of the Mount Harris Basalt, Tjauwata Group, NT.||||||
36943|Mummawarrawarra Basalt|66281|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Unit in Kunmarnara Group.|||Vesicular and amygdaloidal basalt, basaltic andesite and andesite; locally plagioclase porphyritic; epidotised.|
36943|Mummawarrawarra Basalt|66282|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|>1078 Ma.|Unit in Kunmarnara Group.|||Vesicular and amygdaloidal basalt, basaltic andesite, and andesite; locally plagioclase porphyritic; epidotized.|
36943|Mummawarrawarra Basalt|67128|4|Described|p5 Fig.3, p11, p17-19, p28, p31-32|||Western Musgrave Province. Forms significant hills when unmetamorphosed; otherwise low hills or rubbly mounds. Non-magnetic unless strongly metamorphosed. Intruded by c.10km thickness of giant layered mafic-ultramafic sills.|1120-1075 Ma.|Kunmarnara Group.||Conformably overlies MacDougall Formation. Is ovelain by Smoke Hill Volcanics. Is overlain or intruded by Giles intrusions.|A stack of individual 1-5m thick flow units, from amygdaloidal basalt, basaltic andesite (the majority), to andesite. Locally, slightly migmatized to gneiss with alternating layers dominated by fine-grained amphibole or coarser-grained epidote.|
36943|Mummawarrawarra Basalt|67244|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|c.1078 Ma.|Unit in Kunmarnara Group.|||Vesicular and amygdaloidal basalt, basaltic andesite and andesite; locally plagioclase porphyritic; epidotized.|
36943|Mummawarrawarra Basalt|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. ||Unit in Kunmarnara Group.|||Vesicular and amygdaloidal basalt, basaltic andesite, and andesite; locally plagioclase porphyritic; epidotized; locally interleaved and intruded by microgabbro; typically metamorphosed to lower amphibolite facies.|
36943|Mummawarrawarra Basalt|67375|3|Fully described|p19 Fig.11, p38 Table 1, p40, pp216-230|Mesoproterozoic|Mesoproterozoic|Formerly of Tollu Group. Unmetamorphosed, forms significant hills; otherwise, forms low hills, rubbly mounds, or as mesoscopic xenoliths in oldest Giles Suite intrusions. Main outcrops are at MacDougall Bluff (where thickness is about 1100 m), Mummawarrawarra Hill and Mount Blyth. Intruded by a felsic granophyre aged 1078 +/- 4 Ma. Characterized by a strong aeromagnetic (TMI) response, where metamorphosed.|1172 +/- 8 to 1076 +/- 7 Ma.|Unit in Kunmarnara Group.||Conformably overlies MacDougall Formation. Is intruded by oldest mafic intrusions of the Giles Suite. Is overlain unconformably by Tollu Group.|A stack of metre-scale thick, typically basaltic andesite, flow units; massive plagioclase-phyric to highly amygdaloidal; metamorphosed to amphibolite facies near Giles Suite inclusions; epidote alteration very common.|
36943|Mummawarrawarra Basalt|67553|4|Described|p20,37,39-40,42,55,82,84,89|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton.  Type locality: MacDougall Bluff (BLACKSTONE, MGA 437717E 7092336N). Represents the basal succession of the Ngaanyatjarra Rift (Evins et al., 2010). Felsic granophyre interbedded within the basalt dated at 1078+\-4 Ma (crystallisation age; GSWA 183847), providing only direct age constraint on Kunmarnara Group deposition. Intruded by Giles intrusions, and uplifted, eroded, and possibly folded, before deposition of overlying Tollu Group.||Unit of Kunmarnara Group.||Upper unit of Kunmarnara Group. Overlain by Smoke Hill Volcanics/Tollu Group. Underlain by MacDougall Formation.|Amygdaloidal basalts.|
36943|Mummawarrawarra Basalt|68100|5|Briefly described|p5|||||Kunmarnara Group|||Basalt.|
36943|Mummawarrawarra Basalt|68995|5|Briefly described|p6, p47, p48, p59|||||Kunmarnara Group|||Basalts and basaltic andesites.|
36943|Mummawarrawarra Basalt|69091|4|Described|p70, p72, p77, p80, p87-88|||These are basal units of Bentley Supergroup (Howard et al., 2011a; Evins et al., 2010). Mummawarrawarra Basalt forms upper part of Kunmarnara Group.||Kunmarnara Group||Equivalent to Mount Harris Basalt (of Tjauwata Group).|Basalts.|07-OCT-14
36943|Mummawarrawarra Basalt|69153|5|Briefly described|GEOL_LUT_CSV files;GEOCHRON/194421.1.pdf|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen. These zircons are inherited. GEOCHRON/194420.1.pdf.|1186+/-7 Ma (SHRIMP-B, 207Pb/206Pb).|Kunmarnara Group||overlies MacDougall Formation|Vesicular and amygdaloidal basalt, basaltic andesite, and andesite; epidotized; interleaved with and intruded by microgabbro locally; metamorphosed to lower amphibolite facies.|15-AUG-18
36943|Mummawarrawarra Basalt|69436|5|Briefly described|p21:14|||Of Daniels (1974), who assigned it to the Tollu Group. Now assigned to the Kunmarnara Group.||Kunmarnara Group.||Is overlain unconformably by Smoke Hill Volcanics. Correlated with Mount Harris Basalt.||12-JUL-16
36943|Mummawarrawarra Basalt|69655|6|Mentioned|p57-p58|||Mistakenly concatenated as the Mummawarrawarra Formation on p57.||Kunmarnara Group||||
36943|Mummawarrawarra Basalt|69729|5|Briefly described|p74 Fig.8, p79, p87|||Shown as part of the Warakurna Supersuite. Contains abundant garnet porphyroblasts, post-dating the Giles Event.||Kunmarnara Group.||Equivalent to the Mount Harris Basalt.||
36943|Mummawarrawarra Basalt|70619|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Kunmarnara Group|||Massive amygdaloidal plagioclase porphyritic metabasalt; garnet-bearing; locally moderately foliated and amphibolitic.|
36943|Mummawarrawarra Basalt|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|SHRIMP age is derived from basaltic andesite sample (194421.1.pdf) this age is of an inherited component and thus constrains the maximum age for the eruption.|1075 Ma - 1085 Ma (Inferred) 1186 Ma (SHRIMP)|Kunmarnara Group||Nonconformably overlies Macdougall Formation|Vesicular and amygdaloidal basalt to andesite; locally plagioclase porphyritic; epidotized. Interleaved with and intruded by microgabbro; typically metamorphosed to lower amphibolite facies|
36943|Mummawarrawarra Basalt|70763|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Kunmarnara Group.|||Massive amygdaloidal plagioclase-porphyritic metabasalt; garnet-bearing; locally moderately foliated and amphibolitic.|
36943|Mummawarrawarra Basalt|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Forms part of the basal succession of the Ngaanyatjarra Rift (Evins et al., 2010). Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Sample GSWA 194421 (basaltic andesite) yielded an interpreted (weighted mean 207Pb*/206Pb*) maximum eruption age of 1186+\-7 Ma for the Mummawarrawarra Basalt. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv.|1085-1075 Ma (inferred)|Unit of Kunmarnara Group.|||Amygdaloidal basalt to andesite interleaved with and intruded by microgabbro, massive amygdaloidal plagioclase porphyric metabasalt.|
36943|Mummawarrawarra Basalt|70831|5|Briefly described|p2, p6, p11-p12, p22, p26|Stenian|Stenian|Musgrave Province. Deposited during the Giles Event.|c. 1085-1040 Ma|Kunmarnara Group||Overlies the MacDougall Formation.||
36943|Mummawarrawarra Basalt|71210|5|Briefly described|p8, p39-p40|||Estimated thickness of c. 1100m at the MacDougall Bluff locality.||Kunmarnara Group||Equivalent to the Mount Harris Basalt.|Amygdaloidal basalt.|
36943|Mummawarrawarra Basalt|71211|6|Mentioned|p233|||||||||
36943|Mummawarrawarra Basalt|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||basalt, ash tuff|
36943|Mummawarrawarra Basalt|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Typically metamorphosed to lowe amphibolite facies. Sample GSWA 194421 (basaltic andesite) yielded a weighted mean 207Pb/206Pb date of 1186+\-7 Ma, interpreted as inherited zircons and therefore represents maximum age of eruption. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv.|1085-1075 Ma (inferred)|Unit of Kunmarnara Group.||Underlain by MacDougall Formation.|Vesicular and amygdaloidal basalt, basaltic andesite, and andesite; locally plagioclase porphyritic; epidotized; massive amygdaloidal plagioclase porphyritic metabasalt; garnet-bearing; locally moderately foliated and amphibolitic.|
36943|Mummawarrawarra Basalt|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1186+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Basaltic andesite.|
36943|Mummawarrawarra Basalt|72094|5|Briefly described|p17|||Bentley Basin.||Unit of Kunmarnara Group||Underlain by MacDougall Formation. Likely time and lateral equivalent to Mount Harris Basalt.||
36943|Mummawarrawarra Basalt|73437|6|Mentioned|p153|||Deposited at the onset of the Giles Event.||Kunmarnara Group||||
74869|Munarra Monzogranite|64891|5|Briefly described|p37 Fig. 2, p52-53 Tb. 1|Archean|Archean|Of the Tuckanarra Suite. Age: 2670Ma. Geological province: Murchison Domain. Monzogranite; metamorphosed.||||||07-FEB-11
74869|Munarra Monzogranite|69583|5|Briefly described|Plate 2|Neoarchean|Neoarchean|Youanmi Terrane, Yilgarn Craton.||Tuckanarra Suite.|||Metamorphosed granodiorite.|
74869|Munarra Monzogranite|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean|||Tuckanarra Suite|||Monzogranite.|
74869|Munarra Monzogranite|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Tuckanarra Suite.||||
74869|Munarra Monzogranite|70139|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton.||Tuckanarra Suite.|||Granodiorite with minor monzogranite, diorite and microgranite; metamorphosed.|
74869|Munarra Monzogranite|70796|5|Briefly described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton. See also 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, Reedy100_2543_stratig.pdf.|2670 +/ 9 Ma (isotopic)|Tuckanarra Suite|||Monzogranite, with minor granodiorite, diorite, and microgranite; metamorphosed.|
74869|Munarra Monzogranite|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv.|2670+\-9 Ma (isotopic)|Unit of Tuckanarra Suite.|||Monzogranite, with minor granodiorite, diorite, and microgranite; metamorphosed|
74869|Munarra Monzogranite|71271|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton.|c.2670 Ma.|Tuckanarra Suite.|||Monzogranite with minor granodiorite, diorite and microgranite; metamorphosed.|
74869|Munarra Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||2670+/-9 Ma|Tuckanarra Suite|||Monzogranite, with minor granodiorite, diorite, and microgranite; metamorphosed.|
23849|Mundadjini Formation|22589|6|Mentioned|p125||Proterozoic|||||||
23849|Mundadjini Formation|22816|5|Briefly described|p8 Table 1|||Savory Group||||||
23849|Mundadjini Formation|22901|6|Mentioned|76 fig 2|||Geol province Officer Basin||||||
23849|Mundadjini Formation|23156|4|Described|p17|Neoproterozoic|Neoproterozoic|For the location of one of the type areas see p 17.  The Formation has been correlated with the Skates Hills Formation on TRAINOR.  Underlying unit - Spearhole Formation (in type area?).||||||
23849|Mundadjini Formation|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Of Sunbeam Group, Officer Basin.||||||
23849|Mundadjini Formation|23557|5|Briefly described|p95 Fig.1|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||
23849|Mundadjini Formation|23602|4|Described|p17|Neoproterozoic|Neoproterozoic|Age: ~840-815 Ma. Of Savory Group. Overlying unit Boondawari Formation.||||||
23849|Mundadjini Formation|23729|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Savory Group. Geological Province: Savory Basin.||||||
23849|Mundadjini Formation|23730|4|Described|p12|Neoproterozoic|Neoproterozoic|Of Sunbeam Group. O'lying unit Tchukardine Formation. U'lying unit Coondra Formation. Geological Province: Officer Basin.||||||
23849|Mundadjini Formation|23760|4|Described|p30|Neoproterozoic|Neoproterozoic|Of Sunbeam Group. Geological Province: Officer Basin.||||||
23849|Mundadjini Formation|24246|5|Briefly described|p17|Proterozoic|Proterozoic|Overlies Spearhole Formation, overlain by Boondawarrri Formation. Geological Province: Savory Basin.||||||24-FEB-05
23849|Mundadjini Formation|24594|5|Briefly described|p602|Neoproterozoic|Neoproterozoic|Of the Sunbeam Group.  Geological Province: Officer Basin (Paterson Orogen).||||||
23849|Mundadjini Formation|41768|2|Defined|Table 5|Precambrian||||||||
23849|Mundadjini Formation|42708|5|Briefly described|Plate 1|Proterozoic||||||||
23849|Mundadjini Formation|43209|5|Briefly described|map legend||Neoproterozoic|Of Savory Group.||||||
23849|Mundadjini Formation|43229|5|Briefly described|Map Legend||Neoproterozoic|Of Savory Group.||||||30-SEP-08
23849|Mundadjini Formation|43492|3|Fully described|9|||||||||
23849|Mundadjini Formation|43756|4|Described|p535,537|||||||||
23849|Mundadjini Formation|43848|5|Briefly described|Map Legend||Proterozoic|||||||
23849|Mundadjini Formation|44111|6|Mentioned|p.58 Fig. 2, p59|||in Savory Basin. Includes evaporites, stromatolitic carbonates and red beds. Equivalent to Supersequence 1 in Centralian Superbasin.||||||
23849|Mundadjini Formation|50008|5|Briefly described|p46 Fig.3|Neoproterozoic||Of Sunbeam Group. Geological Province: Officer Basin.||||||
23849|Mundadjini Formation|61716|5|Briefly described|p642|Neoproterozoic|Neoproterozoic|Sandstone, mudstone, conglomerate. Informally subdivided in this study into unnamed upper/ lower members separated by 25cm thick silty bed. Exposed around collar of the Glikson impact structure. Age: ~800Ma. Max.thickness: 188m. Geol. Prov: Officer Basin||||||10-MAY-06
23849|Mundadjini Formation|61732|5|Briefly described|p58 Fig. 22|Cryogenian|Cryogenian|Of the Sunbeam Group. Disconformably or unconformably unerlies the Boondawari Formation. Geological Province: western Officer Basin.||||||07-FEB-11
23849|Mundadjini Formation|62453|3|Fully described|p5 Fig. 3, 22, 54-56|Cryogenian|Cryogenian|Of the Sunbeam Group. Geological Province: Officer Basin. Correlated with Browne Formation. Overlies disconformably Spearhole Formation, Coondra Formation. Sandstone, siltstone, conglomerate, shale, dolomite.||||||17-SEP-18
23849|Mundadjini Formation|62987|5|Briefly described|p30|Neoproterozoic|Neoproterozoic|Of the Sunbeam Group. Geological Province: Officer Basin.||||||
23849|Mundadjini Formation|64580|4|Described|map legend||Neoproterozoic|Of Sunbeam Group. Sandstone, siltstone, and minor conglomerate, shale, mudstone, and dolomite (locally stromatolitic); evaporite pseudomorphs.||||||09-DEC-08
23849|Mundadjini Formation|64772|5|Briefly described|p15, p45, Plate 1|Neoproterozoic|Neoproterozoic|Of the Sunbeam Group. Geological province: Officer Basin, Centralian Superbasin. Sandstone, siltstone and minor conglomerate, shale, mudstone, and dolomite (locally stromatolitic); evaporite pseudomorphs.||||||25-NOV-13
23849|Mundadjini Formation|64793|6|Mentioned|p283 fig 2, p285 fig 4|Cryogenian|Cryogenian|Of NW Officer Basin.||||||
23849|Mundadjini Formation|64970|6|Mentioned|p719 Fig. 2|Riphean|Riphean|Geological Province: Officer Basin.||||||27-MAY-09
23849|Mundadjini Formation|65363|6|Mentioned|p5 Fig.4, p10, p19, p37.|Neoproterozoic|Neoproterozoic|May correlate with Lancer Member of the Browne Formation, which has similar large cross-bedding, and possibly with part of the Hussar Formation.||||||
23849|Mundadjini Formation|65365|5|Briefly described|p10 Fig. 4|Cryogenian|Cryogenian|Northwestern Officer Basin||||||
23849|Mundadjini Formation|65366|5|Briefly described|p23 Fig. 3|Cryogenian|Cryogenian|Northwestern Officer Basin||||||
23849|Mundadjini Formation|65410|6|Mentioned|p72.|Neoproterozoic|Neoproterozoic|Savory Basin.||||||
23849|Mundadjini Formation|65416|5|Briefly described|p140.|Neoproterozoic|Neoproterozoic|Correlated with Browne Formation on bases of lithostratigraphy, depositional environments and underlying unconformities. Intertidal, lagoonal and shallow marine environments.|||||Fine- to coarse-grained sandstone, conglomerate, siltstone; minor shale, mudstone and dolomite; occasional poorly preserved stromatolites and evaporite.|
23849|Mundadjini Formation|65454|4|Described|p7 Fig.3, p11, p30 Fig.A1b|Cryogenian|Cryogenian|Of Sunbeam Group. Fine- to coarse-grained sandstone, conglomerate and siltstone; minor shale and mudstone. Overlies Tarcunyah Group. Overlain by Boondawari Formation. Interpreted to be a lateral facies equivalent to Skates Hill Formation.||||||
23849|Mundadjini Formation|67195|5|Briefly described|p10 fig 6, p19 table 1, p45, 48|Neoproterozoic|Neoproterozoic|Savory area, western Officer Basin. Thermal conductivity of 3.80 W/mK. See also App 1, App 2.||||Overlies Spearhole Formation, overlain by Kanpa Formation|Fine grained sandstone interbedded with shale and mudstone; red claystone.|04-JAN-23
23849|Mundadjini Formation|67200|6|Mentioned|app 2 p10||||||||Claystone.|
23849|Mundadjini Formation|67202|5|Briefly described|p64|||NW Officer Basin.|~800 Ma.|Sunbeam Group.||||
23849|Mundadjini Formation|68270|5|Briefly described|p678|||Western Officer Basin. ||||Overlain disconformably by Boondawari Formation.||
23849|Mundadjini Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|NW Officer Basin.||||||
23849|Mundadjini Formation|69185|4|Described|500k_geologyp08_lut.csv||Neoproterozoic|Of Officer Basin.||Unit of Sunbeam Group.|||Undivided; sandstone, siltstone, and minor conglomerate, shale, mudstone, and dolomite (locally stromatolitic); evaporite pseudomorphs|
23849|Mundadjini Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, siltstone, mudstone, sandstone|
23849|Mundadjini Formation|72034|5|Briefly described|500k_interpgeop16_lut|Tonian|Tonian|Officer Basin (Phase 1).  Age from biostratigraphy.||Sunbeam Group|||Sandstone, siltstone, and minor conglomerate, shale, mudstone, and dolomite (locally stromatolitic); evaporite pseudomorphs.|
28828|Mundaring Granite|34115|6|Mentioned|p384|||750 & 590 Ma biotite ages.||||||06-DEC-06
28828|Mundaring Granite|64769|6|Mentioned|p30 Tb. 4, p33, p36 Fig. 24, p118|||Light-medium grey and medium-grained granite. WA.||||||06-MAY-09
81973|Munder Formation|72712|3|Fully described|p9, p22-p30, p35, p38, p43, p44-45.|Paleoproterozoic|Paleoproterozoic|New name. Equivalent to the middle Kazput Formation of Martin et al. (2000). Also previously included in Beasley River Quartzite by others. Approximately 300m thick formation with conglomerate in earliest parts. See also p23, p24, p26, p27, p28, p29, p40 Fig.29, p47.|< c. 2438 Ma MDA.|Turee Creek Group||Unconformably overlies Kazput Formation and Wonangara Member and unconformably underlies Anthiby Formation.|Includes sandstone and conglomerate. Includes succession of medium to coarse-grained, predominantly trough cross-stratified quartz arenite and conglomerate, interpreted to have been deposited on a progradational fluvial braid-plain.|14-JAN-21
80584|Mundine Well Dolerite|72712|5|Briefly described|p9, p35, p38-39, p40.|Tonian|Tonian|Dyke orientation trend varies from north to northeast in the south and west, becoming more generally northeasterly as dykes are traced northeastwards. Previously designated P-d7 (Tyler 1990, 1991). Youngest known dyke suite in the region.|755 +/- 3 Ma.||||Regionally extensive curvilinear swarm of dolerite dykes.|
80584|Mundine Well Dolerite|73102|4|Described|p: 1, 3-4, 6-7, 10-11, 14-20, 28, 30-31|Tonian|Tonian|The most prominent dyke swarm in the Capricorn Orogen; only dykes, no related sills. North to northeast trending. Form an arcuate swarm that extends from the southern Gascoyne Province to the northern Pilbara Craton, concentrated in the west. Strike lengths up to 75 km and are mostly 5-30 m wide, although some dykes are up to 200 m wide. Some thick Mundine Well dykes have melted their host rocks during emplacement. Classified as subalkaline, high-Fe to high-Mg tholeiites. Derived by fractionation of a slightly to moderately enriched mantle source or contamination by evolved or old crustal material. Represent the last known mafic igneous event in the Capricorn Orogen. Intrude Neoarchean-Paleoproterozoic rocks of the Gascoyne Province, Paleoproterozoic metasedimentary rocks of the Ashburton and Blair Basins, Paleoproterozoic to Mesoproterozoic sedimentary rocks of the Edmund Basin, and Mesoproterozoic sedimentary rocks of the Collier Basin. No dolerite sills with similar chemistry have been identified anywhere in the Capricorn Orogen. Similar trend to Kulkatharra Dolerite dykes in the western parts of the Ullawarra and Edmund map sheets, which makes them difficult to distinguish based on orientation alone. Some dykes are locally contaminated with abundant xenoliths of granitic country rock. [Article includes detailed petrographic description, whole rock major and trace element composition, Sm-Nd isotope composition].|c. 755 Ma|||Intrudes sills of the Waldburg, Narimbunna and Kulkatharra Dolerites.|Mainly medium- to coarse-grained quartz- or olivine-normative dolerite, not metamorphosed. Locally contaminated by granitic material.|
80584|Mundine Well Dolerite|74493|6|Mentioned|p3 Fig.2|||||||||
80584|Mundine Well Dolerite|74494|6|Mentioned|p1009|||||||||
41378|Munganbrina Monzogranite|44229|5|Briefly described|Map legend|Archean|Archean|Part of the Mount Edgar Granitoid Complex.  Banded, medium- to coarse-grained monzogranite; locally seriate to porpyritic; foliated.||||||07-NOV-08
41378|Munganbrina Monzogranite|50189|4|Described|p14|Archean|Archean|Formerly the Munganbrina Suite. Oldest and largest pluton of the Mount Edgar Granitoid Complex. Intrudes Mount Ada Basalt and intruded by Chimingadgi Trondjhemite. Monzogranite.||||||07-NOV-08
41378|Munganbrina Monzogranite|50544|4|Described|p30|Archean|Archean|Supersedes the Munganbrina Suite.  Intrudes the Mount Ada Basalt.  Mainly banded, seriate to porphyritic, medium-grained monzogranite with K-feldspar phenocrysts.||||||07-NOV-08
41378|Munganbrina Monzogranite|50555|5|Briefly described|Map legend|Archean|Archean|Of the Mount Edgar Granitoid Complex.  Banded, medium to coarse-grained monzogranite.  Geological Province: Pilbara Craton.||||||18-DEC-12
41378|Munganbrina Monzogranite|60429|4|Described|p6 Fig. 3, p14-15|||Replaced former Munganbrina Suite. Oldest and largest component of Mount Edgar Granitoid Complex. Geol. prov: Pilbara Craton. Consists mainly of banded, seriate to porphyritic, medium-grained monzogranite with scattered, large K-feldspar phenocrysts.||||||07-FEB-11
41378|Munganbrina Monzogranite|63417|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite.  Age: 3310Ma. Geological Province: Pilbara Craton. Monzogranite; banded, medium- to coarse-grained; locally seriate to porhyritic, and weakly foliated; metamorphosed.||||||07-NOV-08
41378|Munganbrina Monzogranite|63420|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite. Geological Province: Pilbara Craton. Banded, medium- to coarse-grained monzogranite; locally seriate to porphyritic; foliated.||||||07-NOV-08
41378|Munganbrina Monzogranite|63441|5|Briefly described|p8 Tb. 2|Archean|Archean|Of Emu Pool Supersuite. Replaces Munganbrina Suite. Age: 3310+/-5Ma. Geological province: Pilbara Craton.||||||07-FEB-11
41378|Munganbrina Monzogranite|64621|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite. Age: c.3310Ma. Monzogranite; banded, medium- to coarse-grained; locally seriate to porphyritic; weakly foliated and metamorphosed.||||||07-NOV-08
41378|Munganbrina Monzogranite|64936|5|Briefly described|map legend|Archean|Archean|Of Mount Edgar Granitoid Complex. Monzogranite. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
41378|Munganbrina Monzogranite|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||Of Mount Edgar Granitoid Complex.|||Banded, medium- to coarse-grained monzogranite; locally seriate to porphyritic; foliated; granitoid rock with mafic and ultramafic xenoliths.|
41378|Munganbrina Monzogranite|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c.3310 Ma.|Of Emu Pool Supersuite.|||Banded, medium- to coarse-grained monzogranite, locally seriate to porphyritic, weakly foliated and metamorphosed; granitic rock with mafic and ultramafic xenoliths, metamorphosed.|
41378|Munganbrina Monzogranite|65827|3|Fully described|p6 Tb.2, p13 Tb.4, p17, p24, p25|Paleoarchean|Paleoarchean|Williams (1999); originally included in Munganbrina Suite (Collins 1983, 1993). Of Emu Pool Supersuite. Of Mount Edgar Granitic Complex. 3310+/-5 Ma (SHRIMP U-Pb zircon; Bodorkos et al. 2006). Intruded by Bishop Creek Monzogranite; intrudes Coppin Gap Granodiorite, Mount Ada Basalt. Contains xenoliths probably from Mount Ada Basalt. Medium- to coarse-grained, biotite monzogranite and granodiorite.||||||
41378|Munganbrina Monzogranite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Emu Pool Supersuite. 3315-3310 Ma. Monzogranite; banded, medium- to coarse-grained; locally seriate to porphyritic; weakly foliated and metamorphosed.||||||
41378|Munganbrina Monzogranite|66217|4|Described|p5, p33, p37.|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Originally Munganbrina Suite (Collins 1983, 1993). Age from U-Pb SHRIMP zircon.|3310 +/- 5 Ma (Bodorkos et al. 2006a).|Unit in Emu Pool Supersuite.||Intrudes Talga Talga and Coongan Subgroups (Pilbara Supergroup). Is intruded by Bishop Creek Monzogranite.|Weakly-foliated, medium- to coarse-grained, biotite monzogranite and granodiorite.|
41378|Munganbrina Monzogranite|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Emu Pool Supersuite.|||Banded, medium- to coarse-grained monzogranite; locally seriate to porphyritic; foliated.|06-JAN-15
41378|Munganbrina Monzogranite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Age derived from sample of monzogranite (178095.1.pdf)|3310 +/- 5 Ma (SHRIMP)|Emu Pool Supersuite|||Monzogranite with mafic and ultramafic xenoliths; weakly metamorphosed. Monzogranite; banded, medium- to coarse-grained; locally seriate to porphyritic; weakly foliated and metamorphosed.|
41378|Munganbrina Monzogranite|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA 178095 (biotite monzogranite) yielded an interpreted igneous crystallisation age of 3310+\-5 Ma for the monzogranite (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3310 Ma (isotopic)|Unit of Emu Pool Supersuite.|||Monzogranite; banded, medium- to coarse-grained; locally seriate to porphyritic, with mafic and ultramafic xenoliths; weakly foliated and metamorphosed.|
41378|Munganbrina Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, amphibolite|
41378|Munganbrina Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||3310+/-5 Ma|Emu Pool Supersuite|||Monzogranite; banded, medium to coarse grained; locally seriate to porphyritic; weakly foliated and metamorphosed.|
35351|Mungarinya Monzogranite|24166|6|Mentioned|p18|Archean|Archean|Age: 2935-2930 Ma (Nelson, 1999)||||||15-APR-13
35351|Mungarinya Monzogranite|50370|5|Briefly described|Map Legend|Archean|Archean|Of Yule Granitoid Complex. Geological Province: Pilbara Craton. Age: c. 2930 Ma||||||07-NOV-08
35351|Mungarinya Monzogranite|50379|5|Briefly described|Map Legend|Archean|Archean|Of Yule Granitoid Complex. Geological Province: Pilbara Craton. Age: c. 2930 Ma.||||||07-NOV-08
35351|Mungarinya Monzogranite|63372|4|Described|Map Legend|Archean|Archean|Of the Yule Granitoid Complex. Geological Province: East Pilbara Granite-Greenstone Terrane. Age: 2938 Ma. Biotite-bearing monzogranite and syenogranite; weakly foliated to massive; metamorphosed.||||||15-APR-13
35351|Mungarinya Monzogranite|63441|5|Briefly described|p11 Tb. 2|Archean|Archean|Of Sisters Supersuite. Replaces Kangan Adamellite. Age: 2938+/-3 Ma. Geological Province: Pilbara Craton.||||||15-APR-13
35351|Mungarinya Monzogranite|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Unit in Sisters Supersuite. c. 2908 Ma. Feldspar(-quartz) porphyritic biotite monzogranite; massive to weakly foliated; locally well developed flow alignment of phenocrysts and schlieren; locally ghost banded; weakly metamorphosed.||||||15-APR-13
35351|Mungarinya Monzogranite|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton. 4 other facies are mapped separately.|c. 2938 Ma|Of the Sisters Supersuite.||Intrudes Siffleetes Granodiorite.|Feldspar(-quartz) porphyritic biotite monzogranite; massive to weakly foliated; locally well developed flow alignment of phenocrysts and schlieren; locally ghost banded; weakly metamorphosed.|30-APR-14
35351|Mungarinya Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Sisters Supersuite|||Feldspar(--quartz) porphyritic biotite monzogranite; massive to weakly foliated; locally well developed flow alignment of phenocrysts and schlieren. Porphyritic monzogranite and pegmatite intruding metagranodiorite.|
35351|Mungarinya Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; North Pilbara Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|2938 Ma (isotopic)|Unit of Sisters Supersuite.||Intrudes into Sifleetes Granodiorite.|Feldspar(-quartz) porphyritic biotite monzogranite; massive to weakly foliated; locally well developed flow alignment of phenocrysts and schlieren; locally ghost banded; weakly metamorphosed, with greenstone xenoliths.|
35351|Mungarinya Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, syenogranite|
35351|Mungarinya Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||2938+/-3 Ma|Sisters Supersuite|||Feldspar(--quartz) porphyritic biotite monzogranite; massive to weakly foliated; locally well developed flow alignment of phenocrysts and schlieren; locally ghost banded; weakly metamorphosed.|
33202|Mungaroona Granodiorite|24533|5|Briefly described|p5 Table 2, p7|Archean|Archean|Of the Yule Granitoid Complex. Age: c.2940Ma (Nelson 2000). Exposed on SATIRIST.||||||07-NOV-08
33202|Mungaroona Granodiorite|24534|5|Briefly described|Map legend|Archean|Archean|Of the Yule Granitoid Complex.  Age: 2935Ma.||||||07-NOV-08
33202|Mungaroona Granodiorite|24554|5|Briefly described|p11|Archean|Archean|Age: c. 2945 Ma (Nelson, 2000)||||||07-NOV-08
33202|Mungaroona Granodiorite|50370|5|Briefly described|Map Legend|Archean|Archean|Of Yule Granitoid Complex. Geological Province: Pilbara Craton. Age: c. 2945 Ma||||||07-NOV-08
33202|Mungaroona Granodiorite|63372|4|Described|Map Legend|Archean|Archean|Of the Yule Granitoid Complex. Geological Province: East Pilbara Granite-Greenstone Terrane. Age: 2945Ma. Hornblende(-biotite)-bearinng granodiorite and monzogranite; greenstone and gneissic rafts and xenoliths; metamorphosed.||||||07-NOV-08
33202|Mungaroona Granodiorite|63441|5|Briefly described|p11 Tb. 2|Archean|Archean|Of Sisters Supersuite. Geological province: Pilbara Craton.||||||07-FEB-11
33202|Mungaroona Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite, monzogranite|
33202|Mungaroona Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||2945+/-5 Ma|Sisters Supersuite|||Hornblende--biotite granodiorite and minor biotite monzogranite; metamorphosed.|
30538|Munglinup Gneiss|22448|5|Briefly described|p875|||||||||
30538|Munglinup Gneiss|23727|4|Described|p52|Archean|Archean|Of Biranup Complex.||||||07-NOV-08
30538|Munglinup Gneiss|23728|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province Albany-Fraser Orogen.||||||
30538|Munglinup Gneiss|23752|4|Described|p11|Archean|Archean|Age: c.2630 Ma. Of Biranup Complex.||||||21-MAR-12
30538|Munglinup Gneiss|23754|5|Briefly described|Map Legend|||Of Biranup Complex. Geological Province Albany-Fraser Orogen.||||||
30538|Munglinup Gneiss|24165|5|Briefly described|p13, p31, Plate 1|Proterozoic|Archean|Reworked fragments of the Yilgarn Craton, deformed and metamorphosed during the Albany-Fraser Orogeny.||Biranup Complex.|||Heterogeneous granitoid gneiss.|
30538|Munglinup Gneiss|24526|5|Briefly described|p105 Fig. 6, p107|Archean|Archean|Of the Biranup Complex. Interleaved with metagabbro and pyroxene granulite of the Fraser Complex.  See also p106 Fig. 7, p112 Fig. 9.||||||07-NOV-08
30538|Munglinup Gneiss|43203|5|Briefly described|Map Legend||Archean|Biranup Complex?||||||07-NOV-08
30538|Munglinup Gneiss|43212|6|Mentioned|p7|||U-Pb SHRIMP of this complex formed at c.2630 Ma.||||||
30538|Munglinup Gneiss|43498|4|Described|4||Proterozoic|U-Pb age: 2630 Ma. Zircon age: 2800Ma||||||
30538|Munglinup Gneiss|62381|4|Described|p2 Fig.2, p6, p11.|||Derived from Archean monzogranite and biotite tonalite. May represent reworked Yilgarn Craton.|Protolith 2640-2575 Ma. Metamorphosed 1250 Ma.|Unit in Biranup Complex.||Intruded by 1300-1280 Ma granite and granodiorite.|Grey biotite orthogneiss derived from a variety of granite, granodiorite and pegmatite protoliths.|30-JUN-14
30538|Munglinup Gneiss|63866|4|Described|p183-p184||Neoarchean|Derived from Archaean monzogranite and biotite tonalite with SHRIMP U-Pb zircon crystallization ages of 2640-2575 Ma. Originally considered part of the Biranup Complex, however Spaggiari et al, 2007 interpreted it as part of the Northern Foreland. Spaggiari et al also provided new SHRIMP U-Pb dates of 2681 +/- 5 Ma, 2661 +/- 15 Ma and 2658 +/- 21 Ma for felsic igneous protoliths of this formation.|2500-1300 Ma|||||
30538|Munglinup Gneiss|64161|6|Mentioned|p578 Fig.1, p582|Neoarchean|Neoarchean|Dated at 2639-2577 Ma by Nelson et al. (1995). Of Biranup Complex. Interpreted to be derived from a granite precursor.||||||21-MAR-12
30538|Munglinup Gneiss|64577|6|Mentioned|p607|||Age: 2640-2575Ma. Felsic.||||||
30538|Munglinup Gneiss|64580|4|Described|map legend|Mesoproterozoic|Neoarchean|Granitic gneiss, heterogeneous; Archean and Proterozoic granitic rock deformed and metamorphosed during Albany-Fraser Orogeny.||||||15-DEC-08
30538|Munglinup Gneiss|64622|5|Briefly described|Map legends|||Geological province: Yilgarn Craton. Granitic gneiss, mainly leucocratic and banded, heterogeneous; Archean granite and greenstone and Proterozoic granitic rock deformed and metamorphosed during the Albany-Fraser Orogeny.||||||15-DEC-08
30538|Munglinup Gneiss|64715|6|Mentioned|p2 Fig. 1|||||||||16-DEC-08
30538|Munglinup Gneiss|64722|5|Briefly described|Fig. 2 p3-6, p18|Neoarchean|Neoarchean|Part of the Biranup Complex of the Albany-Fraser Orogen. Intruded by 1300-1280 Ma granitic rocks.|Protolith age of 2640 - 2575 Ma.||||Felsic orthogneiss.|11-APR-12
30538|Munglinup Gneiss|64771|6|Mentioned|p3 fig 2|||||||||
30538|Munglinup Gneiss|65265|6|Mentioned|p73 Fig.1|||||||||
30538|Munglinup Gneiss|65268|6|Mentioned|p2 Fig.1|||||||||
30538|Munglinup Gneiss|65487|4|Described|p2-3,p11-21,p53-56; Figs.1-2,6-10,27|Gaudalupian|Gaudalupian|Of Myers (1995). A reworked component of the S Yilgarn Craton; part of Northern Foreland, Albany-Fraser Orogen (GSWA, 2007). Formerly part of Biranup Complex. c.2660 Ma; variety of ages is discussed with implications. Amphibolite-granulite facies orthogneisses, interlayered with lenses of metamorphosed mafic rocks; minor jaspilite, amphibolitic schist, serpentinite, and metamorphosed ultramafic rocks.||||||
30538|Munglinup Gneiss|67268|4|Described|p3 , p4 fig 2.1, p5, p20|Neoarchean|Neoarchean|Dominant lithologu in the Northern Foreland province. Ages are similar to that of Yilgarn Craton granites supporting the claim that it may have originally been part of the Yilgarn Craton.|2680 Ma, 2660 Ma,  2630 Ma (Spaggiari et al 2009)||||Amphibolite to granulite facies orthogneiss interlayered with lenses of metamafics, minor metachert, amphibolite schist, serpentinite and metamorphosed ultramafics.|
30538|Munglinup Gneiss|67380|5|Briefly described|p6 Fig.3, p7, p10|Neoarchean|Neoarchean|Northern Foreland, Kepa Burl Booya Province, Albany-Fraser Orogen. U-Pb zircon crystallisation age: this is the oldest known component of the Formation. Another component is dated at 2660 +/- 13 Ma.|2681 +/- 5 Ma (Bodorkos and Wingate, 2008).||||Includes medium- to dark-grey, strongly foliated monzogranitic gneiss with well-developed layering. Amphibolite to granulite facies.|
30538|Munglinup Gneiss|67722|5|Briefly described|p5 fig 2.2, p6, p17, p18|Neoarchean|Neoarchean|Northern Foreland, Albany-Fraser Orogen. Reworked Yilgarn Craton rocks.|Igneous crystallisation 2681 - 2630 Ma||||Moderate to high-strained, ductilely deformed amphibolite to granulite facies metamorphic rocks. Gneisses, granites and dolerite dykes.|07-OCT-16
30538|Munglinup Gneiss|68186|4|Described|p3 Fig.2, p8-13, p19, p28-33, p35, p36|Paleoproterozoic|Neoarchean|See also p42-44, p47, Plate 1A. Myers (1995). Albany-Fraser Orogen. Previously included in the Biranup Complex; reassigned to Yilgarn Craton on bases of geochronological and isotopic data. Bound by major faults. Archean crustal precursors (granites and greenstones) were subject to moderate- to high-strain ductile deformation under amphibolite to granulite facies metamorphism. Local historic Ni deposits. Geochronology and deformation detailed.|c.2709-2630 Ma and c.1299 Ma (protoliths).|||Is intruded by the Gnowangerup-Fraser Dyke Suite.|Dominantly granitic gneiss (granite, granodiorite, tonalite and pegmatite). Also metamorphosed mafic and ultramafic rocks, banded metachert, amphibolitic schist, serpentinite.|
30538|Munglinup Gneiss|68654|5|Briefly described|p2 fig 1, p2, p15 fig 11, p16,17,18,21|||Northern Foreland, Albany Fraser Orogen. Reworked Archean granite. Preserved in thrust sheets. Geochemical data shown and discussed.|2800-2660 Ma|||||
30538|Munglinup Gneiss|69003|6|Mentioned|p28|||||||||
30538|Munglinup Gneiss|69140|6|Mentioned|p2|Neoarchean|Neoarchean|Geological province: Albany-Fraser Orogen.|2800-2660 Ma|||||05-JUL-19
30538|Munglinup Gneiss|69152|5|Briefly described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Neoarchean|Albany-Fraser Orogen|||||Granitic gneiss, heterogeneous, and minor mafic rocks; Archean granite and greenstone and Proterozoic granitic and mafic rock deformed and metamorphosed during the Albany-Fraser Orogeny.|06-AUG-15
30538|Munglinup Gneiss|69252|5|Briefly described|p5, p7-9, p13, p20, p24|||Northern Foreland, Albany-Fraser Orogen. Provenance discussed.|c.2709-2630 Ma.||||Orthogneisses metamorphosed to amphibolite-granulite facies, interlayered with lenses of metamorphosed mafic rocks, with minor banded metachert (jaspilite), amphibolite schist, serpentinite, and metamorphosed ultramafic rocks.|
30538|Munglinup Gneiss|69386|5|Briefly described|p5|||Northern Foreland Zone. A reworked part of the Archean Yilgarn Craton.|2.8-2.6 Ga.||||Predominantly granitic gneiss.|
30538|Munglinup Gneiss|69412|6|Mentioned|p3 Fig.2|||Albany-Fraser Orogen.||||||
30538|Munglinup Gneiss|69414|6|Mentioned|p87|Archean|Archean|Yilgarn Craton. Appears mis-spelled as Mullingup Gneiss.||||||
30538|Munglinup Gneiss|69559|5|Briefly described|500k_geologyp08_lut.csv|Mesoproterozoic|Neoarchean||||||Granitic gneiss, heterogeneous; Archean and Proterozoic granitic rock deformed and metamorphosed during Albany-Fraser Orogeny.|
30538|Munglinup Gneiss|69595|4|Described|p3 fig 1, p4, p5 fig 2, p53|Neoarchean|Neoarchean|Northern Foreland. Protolith ages.|c. 2717-2640 Ma||||Monzogranitic gneiss, biotite monzogranite gneiss, biotite tonalite gneiss, leucocratic granodioritic gneiss, leucocratic tonalite gneiss, migmatitic granitic gneiss.|
30538|Munglinup Gneiss|69743|6|Mentioned|p190|Paleoproterozoic|Paleoproterozoic|||||||
30538|Munglinup Gneiss|70023|5|Briefly described|p167-p168|||Geological province: Albany-Fraser Orogen. Underent HT metamorphism and deformation during Stage II (c. 1225-1140 Ma) Albany-Fraser Orogeny.|2800-2660 Ma|||||17-JUL-19
30538|Munglinup Gneiss|70024|6|Mentioned|p34 Fig.14|||||||||
30538|Munglinup Gneiss|70084|6|Mentioned|p219|Neoarchean|Neoarchean|Geological province: Northern Foreland, Albany-Fraser Orogen, Yilgarn Craton.|2800-2660 Ma|||||
30538|Munglinup Gneiss|70085|6|Mentioned|p234, 241|||Metamorphosed at upper amphibolite to granulite facies c.1190 Ma.||||||
30538|Munglinup Gneiss|70087|6|Mentioned|p213 Fig.1|Archean|Archean|||||||
30538|Munglinup Gneiss|70089|6|Mentioned|p262, 272|Neoarchean|Neoarchean|Northern Foreland, Albany-Fraser Orogen. Protolith ages of 2720-2640 Ma (Spaggiari et al., 2011). Includes a sanukitoid granite aged 2718 +/- 11 Ma, similar age to the Tropicana Zone.|2800-2660 Ma.||||Amphibolite- to granulite-grade orthogneiss.|
30538|Munglinup Gneiss|70090|6|Mentioned|p441-442,445|Neoarchean|Neoarchean|Geological province: Northern Foreland. Higher metamorphic grade component contained within thrust sheets exhumed from a deeper crustal level (Nelson et al., 1995; Spaggiari et al., 2009, 2011, 2014a). |2800-2660 Ma|||||
30538|Munglinup Gneiss|70153|5|Briefly described|100k_geologyp10_lut.csv|Mesoproterozoic|Neoarchean|See also 500k_interpgeop14_lut.csv.|2709 +/- 35 Ma (isotopic) - 1330 Ma (inferred).||||Granitic gneiss, heterogeneous, and minor metamorphosed mafic rocks; Archean granite and greenstone and Proterozoic granitic and mafic rock deformed and metamorphosed during the Albany-Fraser Orogeny.|
30538|Munglinup Gneiss|70156|4|Described|500k_interpgeop14_lut.csv|Mesoproterozoic|Neoarchean|Geological province: Northern Foreland, Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny.|2709+\-35 Ma; 1330 Ma (inferred)||||Granitic gneiss, heterogeneous, and minor metamorphosed mafic rocks; Archean granite and greenstone and Proterozoic granitic and mafic rock deformed and metamorphosed during the Albany--Fraser Orogeny|
30538|Munglinup Gneiss|70182|5|Briefly described|p2-4, p8-15, p21-22,p24-25,p32-34,p45-46|Archean|Archean|Spaggiari et al. (2009, 2011). Northern Foreland, Albany-Fraser Orogen. Orthogneiss protoliths dated at 2720-2640 Ma. Occurs as thrust sheets. Metamorphosed and deformed between 1210 and 1180 Ma. Geochemistry diagrams.|2800-2660 Ma.||||Orthogneiss interlayered with lenses of metamorphosed mafic rocks; minor banded metachert (jaspilite), amphibolitic schist, serpentinite, and metamorphosed ultramafic rocks.|
30538|Munglinup Gneiss|70254|6|Mentioned|p357|||Geological province: Albany-Fraser Orogen.||||||
30538|Munglinup Gneiss|70256|5|Briefly described|p3, p21|||Northern Foreland, Albany-Fraser Orogen. A sanukitoid is dated at 2718 +/- 11 Ma (Kirkland et al., 2013).|2800-2660 Ma.||||Includes sanukitoids.|
30538|Munglinup Gneiss|70732|6|Mentioned|p285|Neoarchean|Neoarchean|Geological province: Albany-Fraser Orogen.|2800-2660 Ma|||||
30538|Munglinup Gneiss|70735|6|Mentioned|p28|||Albany-Fraser Orogen.|2800-2660 Ma.|||||
30538|Munglinup Gneiss|70794|4|Described|500k_interpgeop14_lut.csv|Mesoproterozoic|Neoarchean|Northern Foreland, Albany-Fraser Orogen. Also 2_5m_interpgeop15_lut.csv.|2709+/-39 Ma - 1330 Ma inferred.||||Granitic gneiss, heterogenous and minor metamorphosed mafic rocks; Archean granite, greenstone, proterozoic granitic and mafic rock deformed and metamorphosed during the Albany--Fraser Orogeny|
30538|Munglinup Gneiss|70802|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Neoarchean|Geological province: Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage II (1225-1140 Ma); Albany-Fraser Orogeny (1330-1140 Ma); Albany-Fraser Orogeny Stage I (1330-1260 Ma); Biranup Orogeny (1710-1620 Ma); Ngadju Event (1780-1760 Ma); Salmon Gums Event (1815-1800 Ma). Fault-bounded slice of granulite-facies, dominantly granitic, gneiss. Sample GSWA 184127 (porphyritic monzodiorite) yielded an upper concordia intercept age of 2658+\-21 Ma, interpreted as best estimate of igneous crystallisation age of the monzodiorite. Sample GSWA 184128 (leucocratic tonalitic gneiss) yielded a weighted mean 207Pb*/206Pb* date of 1195+\-17 Ma, interpreted as best estimate of age of zircon recrystallization and rim growth during high-grade metamorphism, likely during Stage II AlbanyFraser Orogeny (1215-1140 Ma; Clark et al., 2000). Sample GSWA 184314 (leucocratic granodioritic gneiss) yielded a weighted mean 207Pb*/206Pb* date of 2661+\-10 Ma, interpreted as best estimate of the igneous crystallisation ag of the granodioritic protolith. Sample GSWA 1843134(migmatitic granitic gneiss) yielded a concordia date of 2709+\-35 Ma and weighted mean 207Pb/206Pb age of 1184+\-6 Ma, interpreted as magmatic crystallisation age and high-grade metamorphism of the granitic protolith respectively. Sample GSWA 192507 (granitic gneiss) yielded a concordia age of 2718+\-11 Ma, interpreted as the magmatic crystallization age of the granite protolith. See 100k_geologyp10_lut.csv, 500k_interpgeop14_lut.csv, 250k_pre_mesozoic_interpgeop_lut.csv.|2709+\-35 Ma; 1330 Ma (inferred)||||Granitic gneiss, heterogeneous, and minor mafic rocks; Archean granite and greenstone and Proterozoic granitic and mafic rock deformed and metamorphosed during the Albany-Fraser Orogeny|
30538|Munglinup Gneiss|70813|5|Briefly described|p3|Neoarchean|Neoarchean|Albany-Fraser Orogen.|c. 2800-2660 Ma|||||
30538|Munglinup Gneiss|70826|6|Mentioned|p9|Neoarchean|Neoarchean|Formed as a resuklt of deformation during late or post Archean tectonism.||||||
30538|Munglinup Gneiss|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||felsic gneiss|
30538|Munglinup Gneiss|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Northern Foreland, Albany-Fraser Orogen. Events: Albany-Fraser Orogeny Stage II (1225 - 1140 Ma); Albany-Fraser Orogeny (1330 - 1140 Ma); Albany-Fraser Orogeny Stage I (1330 - 1260 Ma); Biranup Orogeny (1710 - 1620 Ma); Ngadju Event (1780 - 1760 Ma); Salmon Gums Event (1815 - 1800 Ma). See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv.|2718+\-11 Ma; 2700-1140 Ma (inferred)||||Granitic gneiss, heterogeneous, and minor mafic rocks; Archean granite and greenstone and Proterozoic granitic and mafic rock deformed and metamorphosed during the Albany-Fraser Orogeny|
30538|Munglinup Gneiss|71309|6|Mentioned|p738 Fig.1|||||||||
30538|Munglinup Gneiss|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Neoarchean|Albany-Fraser Orogen.|Max age 2718+/-11 Ma, min age ~1140 Ma.||||Granitic gneiss and minor metamorphosed mafic rocks; intruded by Proterozoic granite and gabbro. Granitic gneiss interlayered with mafic amphibolite; includes intrusions of Paleoproterozoic granitic rocks.|
30538|Munglinup Gneiss|72491|6|Mentioned|p2, 6, 16, 18, 20|Neoarchaean|Neoarchaean|||||||
30538|Munglinup Gneiss|72710|6|Mentioned|p4 Fig.2.|Neoarchean|Neoarchean|Shown as part of the Northern Foreland.|2800 Ma to 2660 Ma.||||Includes gneiss.|
30538|Munglinup Gneiss|73023|6|Mentioned|p2 Fig.1|||||||||
30538|Munglinup Gneiss|73084|6|Mentioned|p12|||Albany-Fraser Orogen, Northern Foreland. Neoarchean protoliths.||||||
30538|Munglinup Gneiss|73168|6|Mentioned|p742 Fig. 3|Archean|Archean|Yilgarn Craton. Albany-Fraser Orogen.||||||
30538|Munglinup Gneiss|73597|6|Mentioned|p1178, 1191, 1192 Fig.10|Archean|Archean|Northern Foreland, Albany-Fraser Orogen. Extensively reworked Archean basement that underplates the Fraser Zone. Trace element data graphed, discussed.|c.2660 Ma.|||||
25310|Mungoo Salt|40837|6|Mentioned|Fig.16|||||||||
37721|Munjina Member|24573|4|Described|p685, 688|||Of the Marillana Formation. Max Thickness: 40m. Contains internal subdivisions: the Basal Conglomerate (upper) and Basal Clay (lower). Geological Province: central Hamersley Range||||||
37721|Munjina Member|60539|5|Briefly described|p498, 500, 501 Fig.3, 513|Miocene|Miocene|Max. age: Middle Miocene. Of the Marillana Formation. Geological Province: Pilbara Craton. Max. thickness: 40 m. Includes conglomerate and clay layers each up to 20 m thick. Underlies: Barimunya Member.||||||
37721|Munjina Member|63432|5|Briefly described| p736 Fig. 3, p750|Middle Miocene|Late Eocene|Basal conglomerate member of the Marillan Formation; overlies Weeli Wolli Formation.||||||07-FEB-11
37721|Munjina Member|65194|5|Briefly described|p107, p110-112|Middle Miocene|Late Eocene|Basal unit in Marillana Formation. Gradationally abuts overlying Barimunya Member. Up to 40m thick and consists of the Basal Conglomerate unit and the Basal Clay unit. Early Oligocene age, suggested from pollen of Nothofagus and other species, is disputed.||||||11-APR-16
37721|Munjina Member|69538|5|Briefly described|p522 Fig.5, p526 Fig.7, p529, p533|Oligocene|Eocene|See also p535, p557 Fig.32, p564, p572-573, p583-585. ||Unit in Marillana Formation.|||Clays and conglomerates; extensive and thick (20-30m) organic units.|
37721|Munjina Member|73574|5|Briefly described|p762|Miocene|Late Eocene|Pilbara Craton. Basal part of the CzD2 sedimentary sequence.||||Underlies Robe Formation in the Western Hamersley, underlies Barimunya Member in the Central Hamersley|Lignite-bearing unit.|
28831|Munkayarra Shale|23765|5|Briefly described|Map Legend|Triassic|Triassic|||||||
28831|Munkayarra Shale|23766|4|Described|p13 Tb. 2|Middle Triassic|Middle Triassic|Consists of multicoloured claystone. Thickness: 185m. See also p26.||||||03-AUG-15
28831|Munkayarra Shale|41688|4|Described|p15|||Reserved as Munkayarra Formation||||||
28831|Munkayarra Shale|43818|6|Mentioned|Fig.2.p39||Middle Triassic|||||||
28831|Munkayarra Shale|64580|4|Described|map legend|Middle Triassic|Early Triassic|Claystone and shale.||||||15-DEC-08
28831|Munkayarra Shale|66949|4|Described|p28, p55 Appx.3|Late Triassic|Middle Triassic|E of Derby. Type section in water bore RGI-2D waterbore 85-270 m. Up to 185m thick; fluvial deposits. Age inferred from position above Erskine Sandstone.||||Conformably overlies Erskine Sandstone.|Multicoloured claystone.|09-OCT-20
28831|Munkayarra Shale|68811|5|Briefly described|p81, p174|Triassic|Triassic|Acts as an aquitard between the Lower Erskine aquifer and the Wallal aquifer near Derby. ||||Overlies the Erskine Sandstone. Overlain by the Wallal Sandstone.||15-APR-20
28831|Munkayarra Shale|69099|5|Briefly described|500k_geologyp08_lut.csv|Middle Triassic|Early Triassic||||||Claystone and shale.|03-AUG-15
28831|Munkayarra Shale|69182|6|Mentioned|Ch4 p3|||Canning Basin. ||||||
28831|Munkayarra Shale|70154|5|Briefly described|500k_interpgeop14_lut.csv|Lower Triassic|Lower Triassic||247-252 Ma||||Claystone and shale|
28831|Munkayarra Shale|71267|6|Mentioned|500k_interpgeop16_lut.csv|Late Triassic|Middle Triassic|Of Canning Basin. Event: Point Moody Extension (300-242 Ma).|247.2-201.3 Ma (inferred)||||Claystone and shale|
28831|Munkayarra Shale|72034|5|Briefly described|500k_interpgeop16_lut|Late Triassic|Middle Triassic|Canning Basin. Age inferred.|||||Claystone and shale.|
37206|Munni Munni Intrusion|23793|6|Mentioned|p30|||||||||
37206|Munni Munni Intrusion|24353|4|Described|p5|Archean|Archean|Intrudes the Cherratta Granitoid Complex. Age: 2925Ma. Max Thickness: 5500m. Geological Province: Pilbara Craton.||||||15-DEC-08
37206|Munni Munni Intrusion|63441|5|Briefly described|p12 Tb. 2, p36, p38|Archean|Archean|Of the Radley Suite. Largest of the funnel-shaped, mafic layered intrusion. Age: 2925+/-16Ma, 2924+/-5Ma. Thickness: ~5.5km. Contains platinum-group elements, nickel and copper. Geological Province: West Pilbara Superterrane.||||||07-FEB-11
37206|Munni Munni Intrusion|64174|5|Briefly described|Map legend|Archean|Archean|Part of the Radley Suite (Sisters Supersuite). Age: c.2925Ma. Gabbro, leucogabbro, serpentinised peridotite and dunite, pyroxenite, and minoranorthosite; metamorphosed.||||||04-DEC-08
37206|Munni Munni Intrusion|64580|4|Described|map legend||Mesoarchean|Of Radley Suite. Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed.||||||15-DEC-08
37206|Munni Munni Intrusion|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological Province: West Pilbara Granite-Greenstone Terrane, Central Pilbara Tectonic Zone, and southwest Pilbara inlier, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 2925 Ma|Unit of Radley Suite.|||Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed|
37206|Munni Munni Intrusion|69299|5|Briefly described|p7, p10 Tb.3, p12, p15, p21|||Of PINDERI HILLS. PGE mineralisation. SHRIMP U-Pb zircon geochronology ages for pegmatite sample (Arndt et al. 1999) and microgranite sample (Nelson 1998), respectively. Specific U-Pb SHRIMP ages on p10 Tb.3.|2925 +/- 16 Ma and 2924 +/- 5 Ma|||||
37206|Munni Munni Intrusion|70775|5|Briefly described|p49, p66, p79-p80|||This is the largest intrusion of the Radley Suite and is roughly 5500m thick. The Munni Munni Intrusion outcrops over an area of 150km ^2 and gravity data indicates an extension concealed by the Fortescue Group. Contains one of the most significant PGE deposits in Australia.|c. 2925 Ma|Radley Suite||Overlain by the Fortescue Group.|Porphyritic plagioclase websterite orthocumulate that overlies ultramafic rocks (dunite, lherzolite, wehrlite, olivine websterite, clinopyroxenite) and is overlain by gabbro.|
37206|Munni Munni Intrusion|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolerite, pyroxcenite, serpentinite|
37206|Munni Munni Intrusion|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||Max age 2925+/-16 Ma, min 2924+/-5 Ma|Radley Suite|||Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed.|
32055|Muntharra Formation|22897|6|Mentioned|102|||Geol province Bangemall Basin. Parent Edmund Group.||||||15-DEC-08
32055|Muntharra Formation|22905|5|Briefly described|p52 Fig. 2, p53 Table 1|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group. Overlying unit: Discovery Formation; underlying unit: Kiangi Creek Formation.  Equivalent to the upper part of the former Jillawarra Formation.  Max. thickness: 50m.||||||24-JAN-06
32055|Muntharra Formation|23403|4|Described|p7|Mesoproterozoic|Mesoproterozoic|Of Edmund Group.||||||
32055|Muntharra Formation|24115|4|Described|p4 Fig.2|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group. Maximum Thickness: 50m. Overlies the Kiangi Creek Formation. Overlain by the Discovery Formation. Geological Province: Edmund Basin.||||||
32055|Muntharra Formation|24183|2|Defined|p1, p14|Calymmian|Statherian|Max. Thickness: 50m. Conformably overlies the Kiangi Creek Formation. Overlain by the Discovery Formation. Age: 1620-1462 Ma.||||||21-MAR-11
32055|Muntharra Formation|24544|4|Described|p44 Fig.32|Mesoproterozoic|Mesoproterozoic|Supersedes Jillawarra Formation. Of Edmund Group. Overlies Kiangi Creek Formation. Overlain by Discovery Formation.||||||
32055|Muntharra Formation|50225|4|Described|p387 Fig. 2, p394|||Of Edmund Gp. Together with Blue Billy Fm replaces part of the former Jillawarra Fm. Dolograinstone, dolomudstone and dolomitic mudstone. Overlain by Discovery Fm; underlain by Kiangi Creek Fm.  Max. thick: 50m. See also p390.||||||07-FEB-11
32055|Muntharra Formation|50380|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin.||||||07-NOV-08
32055|Muntharra Formation|60301|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin. Dolostone and stromatolitic dolostone; sandstone and siltstone.||||||07-NOV-08
32055|Muntharra Formation|63866|5|Briefly described|p162|||||Edmund Group||||
32055|Muntharra Formation|63869|5|Briefly described|p28, p34, p42, p45, Plate 1|Calymmian|Statherian|Martin et al. (1999); Martin and Thorne (2002). 30-50 m thick.|c.1620-1465 Ma.|Unit in Edmund Group.||Conformably overlies Kiangi Creek Formation. Is overlain by Discovery Formation, possibly unconformably.|Thinly bedded, planar-laminated siltstone, dolomitic siltstone, dolostone, with interbedded dolomitic sandstone and quartz sandstone.|
32055|Muntharra Formation|64580|4|Described|map legend||Mesoproterozoic|Of Edmund Group. Siltstone and mudstone; sandstone, and dolostone, minor conglomerate.||||||15-DEC-08
32055|Muntharra Formation|64728|6|Mentioned|p95 Fig.2.|Mesoproterozoic|Mesoproterozoic|Shallow-to deep-marine siliciclastic and carbonate facies.||Unit in Edmund Group.||Overlies Kiangi Creek Formation. Is overlain by Discovery Formation.||
32055|Muntharra Formation|65830|4|Described|p4, p6, p7, p10; Plates 1,2|Calymmian|Statherian|30-50m thick. Restricted to an area immediately adjacent to the Talga Fault. Deposition occurred predominantly below the photic zone, with localized high-energy deposition of carbonate grainstone, dolomitic sandstone, and sandstone.||Of the Edmund Group||Conformably overlies Kiangi Creek Formation. Overlain by the Discovery Formation.|Thinly bedded, planar-laminated siltstone, dolomitic siltstone, and dolostone, with interbedded dolomitic sandstone and quartz sandstone.|
32055|Muntharra Formation|66241|6|Mentioned|pp1-4, p6. |||||Unit in Edmund Group.||Conformably overlies Kiangi Creek Formation. Is overlain disconformably by Discovery Formation.||
32055|Muntharra Formation|69003|5|Briefly described|p34|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||Edmund Group.||Overlies Kiangi Creek Formation. Is overlain by Discovery Formation.||
32055|Muntharra Formation|69024|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Of the Edmund Group.|||Thin- to thick-bedded dolostone and stromatolitic dolostone, and sandstone and siltstone.|05-MAY-14
32055|Muntharra Formation|69027|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Of the Edmund Group.|||Thin- to thick-bedded dolostone and stromatolitic dolostone, and sandstone and siltstone.|05-MAY-14
32055|Muntharra Formation|69028|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin. Mapped with Kiangi Creek Formation as one unit.||Of the Edmund Group.|||Siltstone and mudstone, sandstone, and dolostone; minor conglomerate.|06-MAY-14
32055|Muntharra Formation|69166|4|Described|geologyp_lut.csv|Mesoproterozoic|Paleoproterozoic|||Edmund Group||Overlies Kiangi Creek Formation|Thin- to thick-bedded dolostone and stromatolitic dolostone, and sandstone and siltstone.|
32055|Muntharra Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|||Part of Edmund Group, Depositiional package 3.||Unit of Edmund Group.||||
32055|Muntharra Formation|69596|6|Mentioned|p12 Fig.7|||Edmund Basin.||Edmund Group.||||
32055|Muntharra Formation|70019|6|Mentioned|p93-94|Mesoproterozoic|Mesoproterozoic|Geological province: Gascoyne Province, Capricorn Orogen.||Unit of Edmund Group.||Overlain by Discovery Formation. Underlain by Kiangi Creek Formation.||
32055|Muntharra Formation|70795|4|Described|100k_geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Also 100k_interpgeop_lut.csv, 156614.1.pdf, West Australian Craton, Edmund Basin|1590-1517 Ma|Edmund Group||Overlies Kiangi Creek Formation|Thin to thick bedded dolostone and stromatolitic dolostone, sandstone and siltstone.|
32055|Muntharra Formation|70814|4|Described|p3, p5, p9, p11-p12, p20, p22, p24, p27|||Edmund Basin. Together with the Kiangi Creek Formation forms Depositional Package 3 of the Edmund Group. Attains a maximum thickness of 50m on the Pingandy Shelf. Deposited under quiet-water conditions below storm wave-base. Believed to have been deposited between 1590 and 1517 Ma.||Edmund Group||Conformably overlies the Kiangi Creek Formation. Overlain by the Discovery Formation.|Dolomite and stromatolitic dolomite along with sandstone, dolomitic sandstone and siltstone.|
32055|Muntharra Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||crystalline dolostone/dolomite, dolostone, sandstone, siltstone, mudstone|
32055|Muntharra Formation|72705|5|Briefly described|p3-4|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||Edmund Group.||Overlies Kiangi Creek Formation. Is overlain unconformably by Discovery Formation.|Dolostone; locally developed.|
27211|Murat Siltstone|12498|6|Mentioned|p517 Fig.3. |Early Jurassic|Early Jurassic|||||Overlies North Rankin Formation.||
27211|Murat Siltstone|14227|5|Briefly described|p10|Pleinsbachian|Sinemurian|Geological Province: Exmouth Sub-basin. Marine sedimentation.||||||07-FEB-11
27211|Murat Siltstone|23726|5|Briefly described|p8 Fig 2c|Early Jurassic|Late Triassic|Overlying unit Athol Formation. Underlying unit Mungaroo Formation. Geological Province: Carnarvon Basin.||||||19-SEP-18
27211|Murat Siltstone|24084|5|Briefly described|p146 Fig.2|Early Jurassic|Early Jurassic|Geological Province: North Carnarvon Basin.||||||16-MAR-05
27211|Murat Siltstone|24351|5|Briefly described|Plate 4 (in pocket)|Early Jurassic|Early Jurassic|Geological Province: Exmouth Plateau and Exmouth Sub-basin.||||||13-DEC-07
27211|Murat Siltstone|41438|6|Mentioned|p106|||Reserved as Murat||||||
27211|Murat Siltstone|41732|6|Mentioned|p534|||||||||
27211|Murat Siltstone|41751|2|Defined|p4|Toarcian|Rhaetian|||||||
27211|Murat Siltstone|42116|5|Briefly described|Fig.1 P6|||||||||
27211|Murat Siltstone|42615|4|Described|p28|Pliensbachian|Pliensbachian|||||||
27211|Murat Siltstone|43828|6|Mentioned|p203|||||||||
27211|Murat Siltstone|44937|5|Briefly described|p93|||||||||
27211|Murat Siltstone|50085|5|Briefly described|p23 Fig. 12|Jurassic|Triassic|Geological Province: Northern Carnarvon Basin.||||||
27211|Murat Siltstone|60379|6|Mentioned|p126 fig 3|Middle Jurassic|Early Jurassic|Dampier sub-basin, Carnarvon Basin||||||
27211|Murat Siltstone|60384|6|Mentioned|p244, p243 Fig 2b|Middle Jurassic|Late Triassic|Exmouth Sub-basin, Northern Carnarvon Basin.||||||
27211|Murat Siltstone|60386|6|Mentioned|p300|Early Jurassic|Early Jurassic|Northern Carnarvon Basin. Proximal shelf, distal shelf/basin.||||||
27211|Murat Siltstone|61023|5|Briefly described|p27 Fig. 12|Jurassic|Jurassic|Geological Province: Northern Carnarvon Basin.||||||11-APR-08
27211|Murat Siltstone|62734|5|Briefly described|p1362 Fig. 2|Early Jurassic|Early Jurassic|Geological Province: Barrow Sub-basin.||||||11-APR-08
27211|Murat Siltstone|62837|5|Briefly described|Stratigraphic columns|Early Jurassic|Early Jurassic|Age: ~200-190Ma. Geological Province: Exmouth Sub-basin and Exmouth Plateau.||||||07-NOV-06
27211|Murat Siltstone|63950|5|Briefly described|p336 Fig. 4|Early Jurassic|Early Jurassic|Overlies Brigadier Formation and North Rankin Formation; underlies Athol Formation. Geological Province: northern Carnarvon Basin.||||||27-MAY-08
27211|Murat Siltstone|64978|6|Mentioned|p528 Fig.2.|Early Jurassic|Early Jurassic|||||||
27211|Murat Siltstone|67200|5|Briefly described|p8 fig 6, |Jurassic|Triassic|||||Overlies Mungaroo Formation, overlain by Athol Formation, Learmouth Formation|Siltstone.|
27211|Murat Siltstone|67368|6|Mentioned|p209 Fig.4.|Pliensbachian|Pliensbachian|||||Overlies North Rankin Beds. Is overlain by Athol Formation.||
27211|Murat Siltstone|67970|5|Briefly described|p25 Fig.4.|Toarcian|Pliensbachian|Exmouth Plateau.||||Is overlain by Athol Formation.||
27211|Murat Siltstone|68135|5|Briefly described|p51 fig 2a|Early Jurassic|Early Jurassic|Northern Carnarvon Basin.||||Overlies North Rankin Formation. Is overlain by Athol Formation.||14-SEP-17
27211|Murat Siltstone|69182|6|Mentioned|Ch3 p8, Ch3 p12-p13|||Carnarvon Basin. See also Ch3 p23, Ch3 p35, Ch3 p65-p68, Ch3 p73. ||||||
27211|Murat Siltstone|69297|6|Mentioned|p337, p352|Pleinsbachian|Hettangian|Canning and Roebuck Basins. Overlain by the Depuch Formation equivalents. ||||Overlies the Bedout Formation.||
27211|Murat Siltstone|69689|6|Mentioned|p16|Jurassic|Jurassic|Northern Carnarvon Basin.||||Overlies Athol Formation. Is overlain by Calypso Formation.||
27211|Murat Siltstone|69692|6|Mentioned|p4|Early Jurassic|Early Jurassic|Northern Carnarvon Basin.||||Overlies Brigadier Formation. Is overlain by Athol Formation.||
27211|Murat Siltstone|70065|5|Briefly described|Rowley: Fig.2. Regional: Fig.4|Pliensbachian|Hettangian|Offshore Canning Basin.||||Overlies Bedout Formation. Is overlain by Depuch Formation.||
27211|Murat Siltstone|70066|5|Briefly described|Dampier: Fig.2;p1,p3. Exmouth: Fig.2; p2|Toarcian|Hettangian|See also Regional: Fig.6; p4, p8. Northern Carnarvon Basin. Gas source from fluvio-deltaic sediments; marine sediments are a potential seal.||||Overlies North Rankin Formation. Is overlain by Athol Formation.|Thinly-bedded shelfal siltstone, claystone and marl.|
27211|Murat Siltstone|70906|5|Briefly described|p757 Fig. 2|Jurassic|Jurassic|Gorgon Platform.||||Overlies North Rankin Formation. Is overlain by Athol Formation.||19-SEP-18
27211|Murat Siltstone|73564|5|Briefly described|p1223, 1225|Jurassic|Jurassic|Exmouth Plateau, Gascoyne Margin.||||Overlies North Rankin Formation. Is overlain by Athol Formation.|Shallow- to deep-marine clastic sediments.|
38139|Murgoo Gneiss Complex|23569|6|Mentioned|p3|||||||||
38139|Murgoo Gneiss Complex|24114|5|Briefly described|p6|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
38139|Murgoo Gneiss Complex|24160|6|Mentioned|p64 Fig.26, p112, p114 Fig.50.|||Crops out on western margin of the Murchison Granite-Greenstone Terrane. Appears as Murgoo Gneiss in Fig.26.|||||Pegmatite-banded gneisses, heterogeneous in composition and deformation state.|
38139|Murgoo Gneiss Complex|44149|4|Described|p13, p15, p17, p29-32, p48 |Neoarchean|Mesoarchean|Of SE part of Yilgarn Craton, Western Gneiss Terrane. Derived mainly from granite and other plutonic igneous rocks. Does not include metasediments. Intruded by sheets of granite c.2.7 Ga.. Simpler history than Narryer Gneiss Complex. Age from Wiedenbeck (pers.comm. 1988). Also Rb-Sr whole-rock ages of c.2780-2580 Ma.|c.2650 Ma (Zircon U-Pb).|||Faulted against Narryer Gneiss Complex.|Heterogeneous: pegmatite-banded, generally fine-grained orthogneiss (after granite with pegmatite veins); medium- to coarse-grained, leucocratic biotite granite (intrudes the gneiss).|
73393|Murrin Murrin Formation|65147|5|Briefly described|p4 Fig.3, p5, p5 Fig.4, p6, p15-19   |Neoarchean|Neoarchean|Hosts the Minara nickel mine in smectite and upper saprolite zones in laterite profile.|ca.2698 +/- 5 Ma (Nelson, 2005).|Unit in Minara Group.||Overlies Minerie Formation.|Olivine adcumulate, olivine orthocumulate and gabbro, komatiitic basalts associated with layered mafic-ultramafic cumulates and felsic volcaniclastic rocks.|
73393|Murrin Murrin Formation|65180|4|Described|map legend|Neoarchean|Neoarchean|Metamorphosed basalt, ultramafic rocks and minor sediments. Of the Murrin Domain, Yilgarn Craton. Of Minara Group. Overlies Minerie Formation. Age of c. 2698 Ma given (GSWA geochronology).| Age of c. 2698 Ma given (GSWA geochronology).|||||24-NOV-09
73393|Murrin Murrin Formation|69152|4|Described|minerie_lut. files||Archean|Murrin Domain, Kurnalpi Terrane, Yilgarn Craton|c. 2698 Ma|Minara Group|Includes 9 unnamed subunits.||Serpentinite; basalt with local pyroxene; dacite; epiclastic sandstone; olivine mesocumulates; olivine orthocumulates; olivine adcumulate; pyroxenitic to gabbroic orthocumulate; basalt; all metamorphosed.|06-AUG-15
73393|Murrin Murrin Formation|70153|5|Briefly described|Minerie_100k_geologyp_lut.csv|Archean|Archean|See also minerie_100k_interpgeop_lut. csv. Murrin Domain, Kurnalpi Terrane.|c.2698 Ma.|Minara Group|||Felsic epiclastic sandstone, olivine orthocumulates. Dacite with accretionary lapilli and pumiceous fragments; graded beds and scours; metamorphosed.|
73393|Murrin Murrin Formation|71270|5|Briefly described|GEOL_LUT_CSV files||Archean|Geological province: Murrin Domain, Kurnalpi Terrane, Yilgarn Craton, West Australian Craton. See minerie_100k_geologyp_lut.csv, minerie_100k_geologyl_lut.csv, minerie_100k_interpgeop_lut.csv.||Unit of Minara Group.|||Basalt; coarsely crystalline and pyroxene spinifex-textured; dacite with accretionary lapilli and pumiceous fragments; felsic epiclastic sandstone; olivine cumulates; pyroxenitic to gabbroic orthocumulates; serpentinite.|
23855|Murrouli Basalt|22774|5|Briefly described|p571|||||||||
23855|Murrouli Basalt|23148|5|Briefly described|p112 Table.2|||||||||
23855|Murrouli Basalt|24160|5|Briefly described|p109.|||||Unit in Luke Creek Group.|||A thick pile of tholeiitic and high-Mg basalt.|
23855|Murrouli Basalt|42533|3|Fully described|p10|||Archaean. Name reserved.||||||29-OCT-08
23855|Murrouli Basalt|44149|4|Described|p35 fig 2-30,p36, p42 Fig.2-43|Archean|Archean|See also p45 Fig.2-48, p47, p57 Fig.2-71. Of Murchison Province. Up to 4.4km thick, but patchy due to granite intrusions through it. Contains 5 volcanic and one sedimentary sequences.||Luke Creek Group||Overlain by Golconda Formation.|Thick pile of interlayered tholeiitic and high-Mg basalt.|
23855|Murrouli Basalt|64891|5|Briefly described|p37 Fig. 2, p38, p48-9 Tb. 1|Archean|Archean|Of the Norie Group. Conformable below Yaloginda Fm. Parts intruded by Nannine Tonalite. Age: 2820-2815Ma. Geol.prov: Murchison Domain. A thick succession of pillowed and massive tholeiitic basalt, metamorphosed to amphibolite + upper greenschist facies||||||05-NOV-15
23855|Murrouli Basalt|65268|6|Mentioned|p6 fig 4|||||Luke Creek Group|||Interlayered high-Mg and tholeiitic basalt; minor ultramafic rocks.|
23855|Murrouli Basalt|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c.2820 Ma.|Unit in Norie Group.|||Strongly foliated metabasalt and local amphibolite.|
23855|Murrouli Basalt|67129|5|Briefly described|p18 Fig.19, p47|Archean|Archean|Watkins and Hickman (1990). Murchison Domain, Youanmi Terrane. Also appears as Murroulli dolerite.|2820-2800 Ma|Norie Group|||Tholeiitic and subordinate komatiitic basalts associated with mafic to ultramafic sills.|15-AUG-18
23855|Murrouli Basalt|68110|4|Described|p673, p674 Fig.2|Neoarchean|Mesoarchean|Murchison Domain. Lowermost unit of the Norie Group. A dolerite sill that intrudes this unit has been dated at c. 2792 +/- 2 Ma.|> 2792 +/- 2 Ma.|Of the Norie Group.||Is overlain by Yaloginda Formation.|Komatiites and komatiitic basalts; tholeiitic basalts.|
23855|Murrouli Basalt|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane||Norie Group|Includes 2 unnamed subunits.||Metabasalt and metakomatiitic basalt; local amphibolite; Tremolite--chlorite--talc schist|
23855|Murrouli Basalt|68698|5|Briefly described|p2, p4|Mesoarchean|Mesoarchean|||Norie Group.||Is overlain conformably by Yaloginda Formation.|A thick succession of pillowed and massive tholeiitic basalt.|
23855|Murrouli Basalt|69267|5|Briefly described|p652, 654|||Murchison Province, Yilgarn Craton.||Basal Luke Creek Group.||Is overlain by Golconda Formation.|A thick pile of mafic and ultramafic rocks, with associated gabbro and dolerite sills.|
23855|Murrouli Basalt|69583|4|Described|p47, p49, p157 Fig.7; Plate 2|Mesoarchean|Mesoarchean|Watkins and Hickman (1990). Murchison Domain, western Youanmi Terrane.|c.2820-2800 Ma.|Norie Group.|Mugs Luck Basalt Member.|Is overlain conformably by Yaloginda Formation.|A thick succession of pillowed and massive tholeiitic and komatiitic metabasalts, meta-BIF, meta-ultramafic rock, undivided, typically deeply weathered.|
23855|Murrouli Basalt|69584|5|Briefly described|p2, p5 Fig.2|Mesoarchean|Mesoarchean|||Norie Group|Mugs Luck Basalt|Overlain by the Yaloginda Formation.|Tholeiitic basalt.|
23855|Murrouli Basalt|69586|5|Briefly described|p22-23, p31 Fig.33|Neoarchean|Neoarchean|Murchison Domain. The Cundimurra Granite intrudes near the base of this unit.|c.2820 Ma.|Norie Group.|Mugs Luck Basalt Member.||Tholeiitic and subordinate komatiitic basalts, associated with mafic to ultramafic sills.|
23855|Murrouli Basalt|69627|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton|c. 2820 Ma|Norie Group|||Metabasalt and metakomatiitic basalt.|
23855|Murrouli Basalt|69628|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton|c. 2820 Ma|Norie Group|||Metabasalt and metakomatiitic basalt.|
23855|Murrouli Basalt|70020|4|Described|p117-118|Mesoarchean|Mesoarchean|Geological province: Murchison Domain, Yilgarn Craton. Resulted from a major mantle melting event at c. 2.82 Ga. Thickness: c. 4 km thick.||Unit of Norie Group.|||Interbedded Ti-rich, Al-depleted komatiites and komatiitic volcaniclastic rocks overlain by tholeiitic basalts.|
23855|Murrouli Basalt|70030|5|Briefly described|p192|Mesoarchean|Mesoarchean|Geological province: Murchison Domain, Yilgarn Craton.||Unit of Norie Group.||Overlain by Yaloginda Formation. Underlain (disconformably?) by Golden Grove Formation/Mount Gibson Group.||
23855|Murrouli Basalt|70139|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|2815-2800 Ma.|Norie Group.|||Metabasalt; fine-grained mafic amphibolite schist; strongly foliated metabasalt and local amphibolite; pillowed metabasalt; pyroxene spinifex-textured metabasalt; schistose metakomatiitic basalt; meta-ultramafic rock, typically deeply weathered.|
23855|Murrouli Basalt|70418|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Norie Group.|||Metamorphosed komatiite with relict olivine or pyroxene spinifex texture; strongly foliated metabasalt and local amphibolite; psammitic and pelitic schist interlayered on a metre to decametre scale, locally strongly sheared.|
23855|Murrouli Basalt|70796|5|Briefly described|100k_geologyl_lut.csv|Neoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 198209.1.pdf, Austin100_2442_stratig.pdf, MountMagnet100_2441_stratig.pdf, Nowthanna100_2643_stratig.pdf, Reedy100_2543_stratig.pdf. Numerous additional lithologies are discussed.|ca 2825 to 2800 Ma (inferred)|Norie Group||Overlain by the Yaloginda Formation.|Komatiite with relict olivine spinifex texture; metamorphosed and metabasalt.|
23855|Murrouli Basalt|70830|5|Briefly described|p7, p9, p27-p28|||See also Murroulli dolerite p28.||Norie Group||Conformably overlain by the Yaloginda Formation.|Interbedded, Ti-rich, Al-depleted komatiites and komatiitic volcaniclastic rocks.|
23855|Murrouli Basalt|71168|4|Described|p7-p8, p56|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Emplaced at approximately 2.82 Ga during a major mantle melting event. This unit is approximately four kilometres thick.|c. 2820 Ma|Norie Group||Conformably overlain by the Yaloginda Formation.|Ti-rich, Al-depleted komatiites and komatiitic volcaniclastic rocks that are overlain by tholeiitic basalts.|
23855|Murrouli Basalt|71269|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeol_lut.csv.|2825-2800 Ma|Unit of Norie Group.||Overlain by Yaloginda Formation.|Basalt: pillowed, pyroxene spinifex-textured, metamorphosed; metabasalt and metakomatiitic basalt: strongly foliated, local amphiboite; psammitic and pelitic schist: interlayered, sheared; fine-grained mafic amphibolite schist|
23855|Murrouli Basalt|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|2825-2800 Ma.|Norie Group.|||Metabasalt and metakomatiitic basalt; locally pillowed (mapped separately).|
23855|Murrouli Basalt|71311|5|Briefly described|p795|||Mount Magnet greenstone belt area.|||||Greenstones.|
23855|Murrouli Basalt|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Youanmi Terrane.||Norie Group|||Metabasalt and metakomatiitic basalt.|
23855|Murrouli Basalt|72494|5|Briefly described|p18|||Now included in the Singleton Formation.||||||
31891|Mussel Creek Granite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.||||||07-NOV-08
31891|Mussel Creek Granite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1850Ma. Geological province: Kimberley Province (East).||||||07-FEB-11
31891|Mussel Creek Granite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
31891|Mussel Creek Granite|43854|5|Briefly described|Map Legend||Proterozoic|Of Paperbark supersuite.||||||
31891|Mussel Creek Granite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31891|Mussel Creek Granite|69003|5|Briefly described|p20 Fig.24|Paleoproterozoic|Paleoproterozoic|W zone, Lamboo Province, Halls Creek Orogen.||Paperbark Supersuite.|||Strongly foliated, coarse-grained biotite metamonzogranite.|
31891|Mussel Creek Granite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Paperbark Supersuite|||Medium- to fine-grained, weakly porphyritic biotite metamonzogranite.|03-AUG-15
31891|Mussel Creek Granite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Paperbark Supersuite|||Medium to fine grained, weakly porphyritic biotite metamonzogranite.|
31891|Mussel Creek Granite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone.|1864-1852 Ma (Inferred)|Unit of Paperbark Supersuite.|||Medium- to fine-grained, weakly porphyritic biotite metamonzogranite|
31891|Mussel Creek Granite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1852-1864 Ma|Paperbark Supersuite|||Medium-fine grained, weakly porphyritic biotite metamonzogranite.|
31891|Mussel Creek Granite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (183 -1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1864-1852 Ma (inferred)|Unit of Paperbark Supersuite.|||Medium- to fine-grained, weakly porphyritic biotite metamonzogranite|
31891|Mussel Creek Granite|72437|5|Briefly described|p80, p82|||Lamboo Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Foliated biotite-monzogranite.|
73930|Mutooroo Basalt|62108|5|Briefly described|p1409 Tb. 11|||Of the Kalgoorlie Group. Max. thickness: 200m. Geological Province: Yilgarn Craton (Boulder-Lefroy Shear Zone).||||||07-FEB-11
73568|Myalup Sand|62020|5|Briefly described|p177-190|Pleistocene|Pleistocene|Yalgorup Plain, southern Perth Basin. Moderately diverse fossil foraminifera assemblage (listed). Paleoecological interpretations discussed.|||||Quartz-rich. Contains a fossiliferous limestone lens.|
73568|Myalup Sand|63454|2|Defined|p70, p75|Pleistocene|Pleistocene|Unconformable on Tims Thicket Limestone; unconformable below Kooallup Limestone. Max. thickness:15m. Restricted to Yalgorup Plain. Structureless grey to white quartz sand, mainly fine to med.sand, poorly sorted; upwardly more iron-stained; minor feldspar.||||||
73568|Myalup Sand|73206|4|Described|p856-860, p864-865|Pleistocene|Pleistocene|Of Semeniuk (1997). Yalgorup Plain; restricted to the southern part of the central Swan Coastal Plain. Distinct from Tamala Limestone. Overlain by Myalup Sand Ridge [landform]. Observed as a narrow linear body / barrier dune, extending in coastal length for 40 km and splitting in two in the middle to southern part of the plain. Largely structureless because of Quaternary bioturbation by plants and ants/termites. Low-carbonate cool-water accumulation (supported by modern foram analogues) at a mean sea level around 2-3m below present mean sea level. [Article includes detailed discussion on geoheritage significance].||||Unconformably underlain[?] by Tims Thicket Limestone. Unconformably overlain[?] by Kooallup Limestone.|Limestones and intercalated sediments including quartz sand and shelly calcarenite [lenses].|
35249|Myanna Leucogranite|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Of the Pippingarra Granitoid Complex.  Geological Province: Pilbara Craton.||||||07-NOV-08
35249|Myanna Leucogranite|24110|5|Briefly described|Plate 1|Archean|Archean|Belongs to Pippingarra Granitoid Complex.  Geological Province: Pilbara Craton||||||07-NOV-08
35249|Myanna Leucogranite|24166|4|Described|p17|||Of the Pippingarra Granitoid Complex.||||||25-JUL-07
35249|Myanna Leucogranite|24193|5|Briefly described|p874, p875 Fig.2, p878 Tb.1|Archean|Archean|Parent: Pippingarra granitoid complex. Geological Province: Pilbara Craton. Porphyritic biotite within the Pippingarra granitoid complex.||||||07-NOV-08
35249|Myanna Leucogranite|24327|5|Briefly described|Map Legend|Archean|Archean|Of the Pippingarra Granitoid Complex.Biotite-muscovite monzogranite.  Age: c.2940Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
35249|Myanna Leucogranite|24349|5|Briefly described|Map legend|Archean|Archean|Of the Pippingarra Granitoid Complex.  Age: c.2940Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
35249|Myanna Leucogranite|63420|5|Briefly described|Map legend|Archean|Archean|Of Split Rock Supersuite. Geological Province: Pilbara Craton. Muscovite-biotite monzogranite; locally with quartz and K-feldspar phenocrysts; massive to weakly foliated; metamorphosed.||||||07-NOV-08
35249|Myanna Leucogranite|63441|5|Briefly described|p12 tb. 2|Archean|Archean|Of Split Rock Supersuite. Geological province: Pilbara Craton.||||||07-FEB-11
35249|Myanna Leucogranite|68283|5|Briefly described|Map Legend|Archean|Archean|Pilbara Craton.||Of the Split Rock Supersuite.|||Biotite-muscovite monzogranite; locally with quartz and K-feldspar phenocrysts; massive to weakly foliated; metamorphosed.|23-SEP-13
35249|Myanna Leucogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|Also said to be a constituent of Sisters Supersuite.||Split Rock Supersuite|||Biotite--muscovite monzogranite; locally with quartz and K-feldspar phenocrysts; massive to weakly foliated.|
35249|Myanna Leucogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; Split Rock Supersuite Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|2851-2831 Ma (inferred)|Unit of Split Rock Supersuite.|||Biotite--muscovite monzogranite; locally with quartz and K-feldspar phenocrysts; massive to weakly foliated|
35249|Myanna Leucogranite|70775|5|Briefly described|iv, p71, p80-p81|||Mallina Basin. Poorly exposed over an area of 1000km ^2 south of Port Hedland. Interpreted to be associated with Sn and Ta mineralization at Pippingarra and Bore Creek. May be correlated with the Split Rock Supersuite, however it should be noted that geochronology is required to test this.||Split Rock Supersuite|||Massive to weakly foliated biotite-muscovite monzogranite, locally with quartz and K-feldspar phenocrysts.|
35249|Myanna Leucogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
35249|Myanna Leucogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Biotite--muscovite monzogranite; locally with quartz and K-feldspar phenocrysts; massive to weakly foliated.|
34802|Mystery Monzogranite|22890|6|Mentioned|P13|||||||||
34802|Mystery Monzogranite|22891|6|Mentioned|Map legend||Archean|||||||07-NOV-08
34802|Mystery Monzogranite|24494|5|Briefly described|p38 App.1|||||||||
34802|Mystery Monzogranite|50075|5|Briefly described|p18|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
34802|Mystery Monzogranite|50076|5|Briefly described|Map|Archean|Archean|Fine-grained biotite monzogranite.  Geological Province: Yilgarn Craton.||||||07-NOV-08
34802|Mystery Monzogranite|60076|5|Briefly described|p45 App. 1|||[Agmmy]   Fine-grained, equigranular biotite monzogranite.||||||
34802|Mystery Monzogranite|65264|5|Briefly described|p48 Appdx. 1|Archean|Archean|Fine-grained, equigranular biotite monzogranite.||||||07-FEB-11
34802|Mystery Monzogranite|69152|5|Briefly described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Fine-grained, equigranular biotite monzogranite.|06-AUG-15
34802|Mystery Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|See also 500k_interpgeop14_lut.csv.|2650 - 2600 Ma (inferred).||||Fine-grained, equigranular biotite monzogranite.|
34802|Mystery Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
34802|Mystery Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Vents: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv.|2650 Ma (inferred)||||Fine-grained, equigranular biotite monzogranite|
34802|Mystery Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||||||Fine-grained, equigranular biotite monzogranite.|
23858|Nabberu Supergroup|23589|6|Mentioned|p3|||||||||
23858|Nabberu Supergroup|37460|3|Fully described|p157|||||||||
23858|Nabberu Supergroup|37707|6|Mentioned|Table I|||||||||
23858|Nabberu Supergroup|38978|6|Mentioned|Fig.26|||||||||
23858|Nabberu Supergroup|41997|6|Mentioned|p73|||||||||
31017|Nallana Formation|23455|5|Briefly described|p43|Archean|Archean|3125+/-4Ma||||||07-NOV-08
31017|Nallana Formation|23484|4|Described|p10 table 3|Archean|Archean|Of Whundo Group.  Maximum thickness: 2000m.||||||07-NOV-08
31017|Nallana Formation|23784|5|Briefly described|p10|Archean|Archean|Of Whundo Group (basal unit).||||||07-NOV-08
31017|Nallana Formation|23789|5|Briefly described|p9 Tb. 2|Archean|Archean|Parent: Whundo Group.  Max. thickness: 2000m.  Age: 3125+/-4Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
31017|Nallana Formation|23793|4|Described|p16|Archean|Archean|Of Whundo Group. See also page 11 table 2||||||07-NOV-08
31017|Nallana Formation|23794|5|Briefly described|Map Legend|Archean|Archean|Of Whundo Group. Overlying unit Tozer Formation. Geological Province: Pilbara Craton.||||||07-NOV-08
31017|Nallana Formation|24023|5|Briefly described|p7 fig. 4|Archean|Archean|Of Whundo Group. Maximum thickness: 2000m.||||||07-NOV-08
31017|Nallana Formation|24184|4|Described|p712 Tb.2|Archean|Archean|Of the Whundo Group. Overlain by Tozer Formation. Geological Province: Pilbara Craton. Max Thickness: 2000m. Age: 3125 +/- 4Ma (Nelson 1996)||||||07-NOV-08
31017|Nallana Formation|24353|4|Described|p9 Fig.5, p11 Tb.2|Archean|Archean|Of the Whundo Group. Age: 3125 +/- 4Ma. Max Thickness: 2000m. Geological Province: Pilbara Craton||||||07-NOV-08
31017|Nallana Formation|24541|3|Fully described|p11 Tb.2, p22|Archean|Archean|Of the Whundo Group. Age: Felsic tuff dates at 3125+/-4 Ma. Base of formation intruded by 3130 Ma granitoids. Overlain by the Tozer Formation.||||||07-NOV-08
31017|Nallana Formation|24543|5|Briefly described|Map legend|Archean|Archean|Of the Whundo Group (Pilbara Supergroup).  Age: c. 3125Ma.  Felsic volcanic rock.||||||07-NOV-08
31017|Nallana Formation|24550|5|Briefly described|p36 Tb. 3.2|Archean|Archean|Of the Whundo Group. Mainly basalts, minor ultramafics, and intermediate pyroclastics. Overlain by Tozer Formation. Age: ca 3125Ma. Thickness: 2km. Geological Province: Pilbara Craton. See also p39.||||||07-FEB-11
31017|Nallana Formation|61253|5|Briefly described| p52 Fig. 2|Archean|Archean|Age: >3.1Ga. Geological Province: Pilbara Craton.||||||07-NOV-08
31017|Nallana Formation|63372|4|Described|Map Legend|Archean|Archean|Of the Whundo Group. Geological Province: West Pilbara Granite-Greenstone Terrane. Age: 3125Ma. Basalt, with minor ultramafic, felsic, and sedimentary units; metamorphosed.||||||07-NOV-08
31017|Nallana Formation|63441|4|Described|p5 Tb.1, p24|Archean|Archean|Lowest unit of Whundo Group (Pilbara Supergroup). Conformably overlain by Tozer Formation. Thickness: >2000m. Geological province: West Pilbara Superterrane. Comprises metabasalt, ultramafic rocks, intermediate pyroclastic rocks, and dolerite sills.||||||07-FEB-11
31017|Nallana Formation|63538|5|Briefly described|p6 Fig. 3|Archean|Archean|Of Whundo Group. Overlain by Tozer Formation. Geological Province: Pilbara Craton.||||||19-APR-13
31017|Nallana Formation|64174|5|Briefly described|Map legend|Archean|Archean|Of the Whundo Group. Age: 3125Ma. Metabasalt with minor metamorphosed ultramafic, felsic and sedimentary units; metamorphosed.||||||07-NOV-08
31017|Nallana Formation|64580|4|Described|map legend||Mesoarchean|Of Whundo Group. Metabasalt, with minor metamorphosed ultramafic, felsic, and sedimentary units; metamorphosed.||||||15-DEC-08
31017|Nallana Formation|64632|6|Mentioned|p203 Fig.2|||||Of the Whundo Group.||Overlain by the Tozer Formation.||
31017|Nallana Formation|67201|4|Described|p7 Fig.4, p12 Tb.1, p15-18|Archean|Archean|In northwestern Pilbara Craton, West Pilbara Superterrane, Sholl Terrane, Whundo Basin. Thickness: > 2 km.|c. 3126 Ma|Whundo Group||Is conformably overlain by Tozer Formation.|Metabasalt; with minor metamorphosed ultramafic, intermediate pyroclastic rocks, dolerite sills, felsic and sedimentary units.|
31017|Nallana Formation|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological province: West Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 3125 Ma|Unit of Whundo Group.|||Metabasalt, with minor metamorphosed ultramafic, felsic, and sedimentary units; metamorphosed|
31017|Nallana Formation|69299|5|Briefly described|p5 Fig.4, p6 Tb.1, p11|||Thickness on COOYA POOYA: 200 m. Base of formation intruded by 3130 Ma granitoids and truncated by Maitland Shear Zone.|3125 +/- 4 Ma|Of Whundo Group. |||Dominantly basalt.|01-JUL-14
31017|Nallana Formation|69300|5|Briefly described|map legend|Archean|Archean|West Pilbara Granite-Greenstone Terrane. Isotopic age: shown on legend as c. 3125 Ma|3125 +/- 4 Ma (isotopic age, Nelson 1996)|Whundo Group|||felsic volcanic rock and basalt; metamorphosed|
31017|Nallana Formation|69301|4|Described|p5 Fig.3, p9 Tb.1, p14|||Pilbara Craton. West Pilbara Superterrane. Whundo Basin. Sholl Terrane. Thickness: >2.0 km.|3126 Ma|Lowest formation in Whundo Group||Is conformably overlain by Tozer Formation.|Mafic volcanic rocks. Comprises metabasalt, ultramafic rocks, intermediate pyroclastic rocks, and dolerite sills.|
31017|Nallana Formation|70022|6|Mentioned|p115|||West Pilbara Superterrane.||Whundo Group.||||
31017|Nallana Formation|70775|4|Described|p12, p15, p24||Mesoarchean|Whundo Basin. This unit is more than 2000m thick. Lithology is discussed more broadly. See also  p25 tbl 4, p32-p34 , p37, p41, p74.|3130-3128 Ma|Whundo Group||Conformably overlain by the Tozer Formation. Intruded by the Bullock Hide Intrusion.|Metabasalt with minor metamorphosed ultramafic, felsic and sedimentary units.|
31017|Nallana Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Whundo Basin.||Whundo Group|||Basalt with minor ultramafic, felsic, and sedimentary units; metamorphosed.|
31017|Nallana Formation|72251|5|Briefly described|p54|Mesoarchean|Mesoarchean|Geological province: Sholl Terrane, West Pilbara Superterrane, Pilbara Craton.||Unit of Whundo Group.||Overlain by Tozer Formation or Cleaverville Formation. Underlain by Regal Formation.||
31017|Nallana Formation|72668|6|Mentioned|p4, p12|||West Pilbara Superterrane.||Whundo Group||Overlain by the Tozer Formation.||
26070|Nambeet Formation|7433|6|Mentioned|p25 Fig.2, p28 Fig.5. |Ordovician|Ordovician|Canning Basin. Fine clastics; marine.||||||
26070|Nambeet Formation|13255|6|Mentioned|p368|Early Ordovician|Early Ordovician|Roebuck Basin.||||Is overlain by Willara Formation.||
26070|Nambeet Formation|13995|5|Briefly described|p67-68, p87|Ordovician|Ordovician|Canning Basin. Graptolite species.||||||
26070|Nambeet Formation|14228|5|Briefly described|p6 fig3|Early Ordovician|Early Ordovician|Canning Basin.||||Overlain by Willara Formation.||05-OCT-16
26070|Nambeet Formation|22646|6|Mentioned|Fig 5 on p 105|Early Ordovician||Canning Basin.||||||
26070|Nambeet Formation|22655|6|Mentioned|p 269|||Province - Kidson Sub-basin (Canning Basin) p269.||||||
26070|Nambeet Formation|22718|5|Briefly described|P4, Table1 P7||Early Ordovician|||||||
26070|Nambeet Formation|22738|4|Described|11,12, map|Early Ordovician|Early Ordovician|Max thickness 800 m. Overlain by Grant Group, Willara Formation.||||||13-NOV-07
26070|Nambeet Formation|22741|6|Mentioned|p21|||||||||11-FEB-20
26070|Nambeet Formation|22753|5|Briefly described|Fig.3 p585|Ordovician|Ordovician|||||||
26070|Nambeet Formation|22765|5|Briefly described|P7, Table1||Arenig|Maximum thickness 71m||||||
26070|Nambeet Formation|22767|5|Briefly described|Table3 P18, P10||Early Ordovician|||||||
26070|Nambeet Formation|22801|5|Briefly described|P10, Table1 P9||Early Ordovician|||||||
26070|Nambeet Formation|22814|5|Briefly described|fig2|Early Ordovician|Early Ordovician|||||||
26070|Nambeet Formation|23212|4|Described|Table.1 p6||Early Ordovician|Fossil assemblage in NF outside M.Hills mapping area indicates E.Ordovician-Late Cambrian Age.||||||13-NOV-07
26070|Nambeet Formation|24061|4|Described|p175|Early Ordovician|Early Ordovician|Geological Province:  Canning Basin.||||||
26070|Nambeet Formation|24062|5|Briefly described|p186 Table 1|Ordovician|Ordovician|Geological Province: Canning Basin.||||||
26070|Nambeet Formation|24390|5|Briefly described|p6 Fig. 4|Ordovician|Ordovician|Geological Province: Canning Basin.||||||
26070|Nambeet Formation|24449|5|Briefly described|p741 Fig. 2|Arenigian|Tremadocian|Age: ~500m.y.  Geological Province: Canning Basin.||||||05-OCT-16
26070|Nambeet Formation|30110|6|Mentioned|p81|||See also P82. Tremadocian age.||||||
26070|Nambeet Formation|30313|4|Described|p54|||Lower Ordovician age||||||
26070|Nambeet Formation|30595|5|Briefly described|p3|||||||||
26070|Nambeet Formation|31047|6|Mentioned|Fig. 2|||Stratigraphic section through Canning Basin.||||||
26070|Nambeet Formation|31572|14|Not recorded|p.22.||Early Ordovician|Correlation Chart 1.||||||
26070|Nambeet Formation|32648|6|Mentioned|p32|||Cambrian-Ordovician||||||
26070|Nambeet Formation|33738|6|Mentioned|p47|||||||||
26070|Nambeet Formation|33965|4|Described|Table 1|||||||||
26070|Nambeet Formation|35119|4|Described|p466|||Mention Text-Fig.3.||||||
26070|Nambeet Formation|35275|6|Mentioned|Fig.5|||||||||
26070|Nambeet Formation|36438|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
26070|Nambeet Formation|36634|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
26070|Nambeet Formation|36890|3|Fully described|p323|||||||||
26070|Nambeet Formation|37368|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
26070|Nambeet Formation|37369|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
26070|Nambeet Formation|37370|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
26070|Nambeet Formation|38878|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
26070|Nambeet Formation|38886|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
26070|Nambeet Formation|39857|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
26070|Nambeet Formation|40078|6|Mentioned|Map legend|Middle Ordovician|Early Ordovician|Early to Middle OrdovicianE - M||||||
26070|Nambeet Formation|40136|5|Briefly described|p33|||||||||
26070|Nambeet Formation|40992|6|Mentioned|Fig.11|||||||||
26070|Nambeet Formation|41169|6|Mentioned|p140|||See also Fig. 3||||||
26070|Nambeet Formation|41215|6|Mentioned|p265|||See also Fig.5||||||
26070|Nambeet Formation|41730|6|Mentioned|Fig.3|||||||||
26070|Nambeet Formation|41854|5|Briefly described|p94|||||||||
26070|Nambeet Formation|42347|6|Mentioned|Fig.2 P1020|||||||||
26070|Nambeet Formation|42880|5|Briefly described|Fig.2,p1020|||||||||
26070|Nambeet Formation|42930|5|Briefly described|Fig.1 p473|Early Ordovician|Late Cambrian|Unconformably overlies a Late Cambrian basement; conformably overlain by Willara Formation. Geological Province: Canning Basin.||||||13-NOV-07
26070|Nambeet Formation|43173|6|Mentioned|11-54||Ordovician|||||||
26070|Nambeet Formation|43563|6|Mentioned|p4|||||||||
26070|Nambeet Formation|43599|6|Mentioned|p251|||||||||
26070|Nambeet Formation|43656|6|Mentioned|Fig.2,p8|Arenigian|Tremadocian|||||||
26070|Nambeet Formation|43666|6|Mentioned|p19||Tremadoc|||||||
26070|Nambeet Formation|43746|6|Mentioned|Fig.2,p11|Arenigian|Tremadocian|||||||
26070|Nambeet Formation|43803|6|Mentioned|p65||Ordovician|||||||
26070|Nambeet Formation|43815|6|Mentioned|Table 1,p95-96|||||||||
26070|Nambeet Formation|43818|6|Mentioned|Fig.2.p39||Early Ordovician|||||||
26070|Nambeet Formation|43825|6|Mentioned|p144|||||||||
26070|Nambeet Formation|44143|4|Described|p426, p428 p441 Table 4-19|Early Ordovician|Early Ordovician|Up to 775m thick; shale, limestone & dolomite; shallow marine. Passes laterally into Wilson Cliffs Sandstone. Tremadocian(?) to Arenigian. Type section between 1240 and 2015m in Samphire Marsh 1 (MANDORA: 19deg 31' 08" S, 121deg 10' 51" E).||||||23-NOV-17
26070|Nambeet Formation|44356|6|Mentioned|p8||Early Ordovician|||||||
26070|Nambeet Formation|44357|5|Briefly described|p11,Tb.1 p10||Early Ordovician|Assumed present from seismic evidence and drilling in adjacent sheets.||||||
26070|Nambeet Formation|45153|2|Defined|App.1-1|Early Ordovician|Early Ordovician|||||||
26070|Nambeet Formation|45158|3|Fully described|p28|||||||||
26070|Nambeet Formation|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
26070|Nambeet Formation|48971|6|Mentioned|p33|||||||||
26070|Nambeet Formation|50085|5|Briefly described|p6 Fig. 4|Ordovician|Ordovician|Geological Province: Canning Basin.||||||
26070|Nambeet Formation|50089|5|Briefly described|p430 Fig. 5|Ordovician|Ordovician|Contains Oepikodus cleftus (conodont) in upper level. Geological Province: Canning Basin. See also p431.||||||
26070|Nambeet Formation|61021|5|Briefly described|p36 Fig. 2|Arenigian|Tremadocian|Geological Province: Canning Basin.||||||17-DEC-07
26070|Nambeet Formation|61023|5|Briefly described|p10 Fig. 6|Ordovician|Ordovician|Geological Province: Canning Basin.||||||11-APR-08
26070|Nambeet Formation|61551|6|Mentioned|p351 Fig.2. |Tremadocian|Tremadocian|||||Is overlain by Willara Formation.||
26070|Nambeet Formation|62982|5|Briefly described|p7|Ordovician|Ordovician|Coarse clastics. Overlain by Willara Formation. Geological Province: Canning Basin.||||||16-JAN-07
26070|Nambeet Formation|64185|5|Briefly described|p158 Fig. 2, p162-163, p166|Early Ordovician|Early Ordovician|Overlain by Willara Formation, conformably. Max thickness:410m. Shallow marine. See p162-163 for more information on lithology.||||||
26070|Nambeet Formation|64186|4|Described|p169, p170 Fig. 1|Early Ordovician|Late Cambrian|Overlain by Willara Formation. Max thickness: 100m Was deposited as a transgressive sand sheet over an irregular basement surface.||||||05-OCT-16
26070|Nambeet Formation|64334|5|Briefly described|p39-41, 43|Ordovician|Ordovician|Canning Basin; subsurface only. Tremadoc-Arenig.||||Is overlain by Willara Formation. Correlated with Prices Creek Group and Carranya Formation.|Sandstone, mudstone. Fossiliferous.|
26070|Nambeet Formation|64513|6|Mentioned|p34 Fig4.|Early Ordovician|Early Ordovician|Canning Basin. Mentioned in p34 Fig.4 with respect to faunal zones.||||Underlies Willara Formation.|Includes fossiliferous rock.|
26070|Nambeet Formation|64643|5|Briefly described|p3 Fig. 2|Middle Ordovician|Lower Ordovician|||||||
26070|Nambeet Formation|64982|5|Briefly described|p695, pp702-703.|Tremadocian|Tremadocian|South Canning Basin. 230 - 400 m thick transgressive unit with graptolites, trilobites, brachiopods, conodonts and gastropods. Gas indicated in low porosity sandstones over two intervals. ||||Is overlain by Willara Formation.|Sandstones, interbedded shales, limestones and dolomites.|
26070|Nambeet Formation|65301|5|Briefly described|p3, p5 Fig. 4|Middle Ordovician|Early Ordovician|Geological province: Canning Basin, Broome Platform. Includes sandstones. See also p8 Fig. 5.||||||
26070|Nambeet Formation|65449|5|Briefly described|p3, p5-6|Middle Ordovician|Early Ordovician|Fossiliferous marine unit. Base of Megasequence I of Warris (1993).||||Is overlain by Willara Formation. Lateral equivalent of Wilson Cliffs Sandstone.|Includes widespread basal siliciclastics.|
26070|Nambeet Formation|68007|5|Briefly described|p2, p4, p15, Plate 1|Middle Ordovician|Early Ordovician|Canning Basin. Fossiliferous marine unit.||||Is overlain by Willara Formation. Equivalent to top part of Wilson Cliffs Sandstone.||25-FEB-20
26070|Nambeet Formation|68902|5|Briefly described|p8, p9, p24, p26|Ordovician |Ordovician |SW Canning Basin. Intersected in Samphire Marsh 1 drillhole.||||Overlain by Willara Formation and Grant Group.||
26070|Nambeet Formation|69029|6|Mentioned|p319|Tremadocian|Tremadocian|Of Canning Basin.||||Overlain by Willara Formation.||
26070|Nambeet Formation|69182|5|Briefly described|Ch4 p9-p12, Ch4 p20-p25|Early Ordovician|Early Ordovician|Canning Basin. Claystones within this formation are good potential seals for the storage of carbon dioxide. Very little prospectivity as a carbon dioxide reservoir due to poor porosities. See also Ch4 p30-p36, Ch4 p39-p41, Ch4 p44-p45, Ch4 p47-p48, Ch4 p50-p58, Ch4 p62-p65, Ch4 p67, Ch4 p71, Ch4 p74, Ch4 p79-p82, Ch4 p92-p94.  ||||Overlain by the Willara Formation.|Basal sandstone overlain by claystones with minor carbonates.|11-FEB-20
26070|Nambeet Formation|69297|6|Mentioned|p350|Early Ordovician|Early Ordovician|Canning Basin. Deposited under marine or supratidal conditions.||||||
26070|Nambeet Formation|69312|5|Briefly described|p3, p23 fig 26, p24 fig 28|Early Ordovician|Early Ordovician|Canning Basin. See also  p25 fig 30, p26 fig 32, p27 fig 34, p28 fig 36.||||Overlain by the Willara Formation.|Carbonate shales, marl.|11-FEB-20
26070|Nambeet Formation|69883|4|Described|p1, p4-p6, p14, |Arenig|Tremadocian|Canning Basin. Deposited in a marine environment. Contains potential petroleum source rocks, however Edwards et al (1997) considered these of limited potential. Age equivalent to the Wilson Cliffs Sandstone. See also p22, plate 2-4.||||Conformably overlain by the Willara Formation. Coeval with the Wilson Cliffs Sandstone.|Basal transgressive sandstone and conglomerate, succeeded by mudstone, limestone, dolostone and sandstone of a marine origin.|27-FEB-20
26070|Nambeet Formation|70774|5|Briefly described|p4|Middle Ordovician|Early Ordovician|Willara and Kidson Sub-basins, Canning Basin.||||Overlain by the Willara Formation. Equivalent to the Wilson Cliffs Sandstone.||06-FEB-20
26070|Nambeet Formation|71146|5|Briefly described|p6, p24, p26|Middle Ordovician|Early Ordovician|Canning Basin. Thickness exceeds 775m in Samphire Marsh 1.||||Overlain by the Willara Formation. Equivalent to the Kudata Formation.|Sandstone, conglomerate, carbonate and mudstone.|
26070|Nambeet Formation|71171|6|Mentioned|p1-p2, p4-p5, p18|||Canning Basin.||Prices Creek Group||Laterally equivalent to the Wilson Cliffs Sandstone.||
26070|Nambeet Formation|71870|4|Described|p1-p3, p5-p16|Floian|Tremadocian|Canning Basin. The type section for this unit is intersected in Samphire Marsh 1. This unit was first proposed in Johnstone, 1966 and Koop, 1966. The unit was first formally defined by Playford et al.., 1975 and thereafter subdivided in the Broome Platform by Bellis (1987). Intersected in the Olympic 1 petroleum well where it displays good petroleum source quality. Unconformably overlies precambrian granite, gneiss and sedimentary basement rocks of the Canning Basin.||||Overlain by the Willara Formation. Unconformably overlain by the Grant Group. Equivalent to the Prices Creek Group and Wilson Cliffs Sandstone.|Dark-grey mudstones interbedded with light-grey carbonates overlying basal fine-grained, subarkosic sandstone.|
26070|Nambeet Formation|71894|5|Briefly described|p3-p4, p20|Early Ordovician|Early Ordovician|Canning Basin.||||Overlain by the Willara Formation.|Cabonate and shale.|11-FEB-20
26070|Nambeet Formation|72497|5|Briefly described|p3 Fig.2.|Early Ordovician|Early Ordovician|Shown as occuring in the Anketell, Tabletop, Ryan Shelves, Willara and Kidson Sub-basins, the Jurgurra and Barbwire Terraces and Broome Platform. Also possibly shown as occuring in the Fitzroy Trough, Betty and Balgo Terraces.||||Conformably underlies Willara Formation and unconformably underlies Wilsons Cliffs Sandstone.||
26070|Nambeet Formation|72499|5|Briefly described|p7 Fig.6.|Early Ordovician|Early Ordovician|Located in the Willara Sub-basin and the Broome Platform.||||Underlies Willara Formation and is laterally equivalent to Wilson Cliffs Sandstone.|Includes carbonate shales.|
26070|Nambeet Formation|72500|4|Described|p379-386, p389-391, p393-399, p401-402|Floian|Tremadocian|Canning Basin. Type section occcurs between 1240 and 2015m in the Samphire Marsh 1 well in the Willara Sub-basin. Hosts a well-preserved and moderately diverse microphytoplankton assemblage which consists of: prasinophyte phycomata, acritarchs, cyanobacteria, degraded algae, chitinozoans and graptolite fragments. Unconformably overlies the Precambrian and Cambrian basement in the Canning Basin. Deposited in a low energy, offshore, normal marine environment with periodic regressions.||||Conformably overlain by the Willara Formation.|Basal sandstone bollowed by beds of varying thickness of limestone, dolostone, shale, siltstone and interbeds of sandstone.|28-AUG-20
26070|Nambeet Formation|72503|6|Mentioned|p27|||Canning Basin.||||Overlain by Willara Formation.|Includes dolostone, mudstone, and sandstone.|
26070|Nambeet Formation|73117|5|Briefly described|p3|Lower Ordovician|Lower Ordovician|Canning Basin. Lower boundary marked by a major unconformity[?] [related to the Samphire Marsh Movement?].||||Overlain by Willara Formation. Equivalent to Wilson Cliffs Sandstone.|Upper portion is dominantly carbonate-shale, marl; lower portion is dominantly sandstone.|
26070|Nambeet Formation|73344|3|Fully described|p. 1-15, 18, 21, 29-33, 35-44, 46-47...|earliest Dapingian|Tremadocian|Canning Basin, northwestern and central. Known only from the subsurface. Defined by Playford et al. (1975). Type section designated from Samphire Marsh 1 petroleum exploration well, but only from 12.6 m of core recovered from 8 separate intervals between 1240 and 2015 m [775 m unit thickness]. Authors indicate the type section is unsatisfactory and that the unit is atypically thick in that well. A reference section is proposed from the Olympic 1 petroleum exploration well, which includes a 277.53 m interval of the unit. Base of the unit is predicted to be 20 m below the base of the well. Seven bentonite U-Pb zircon CA-ID-TIMS dates range from 479.37 +/- 0.18 Ma at the base of the Samphire Marsh Member to 470.18 +/- 0.13 Ma in the lowermost Willara Formation (Normore et al., 2018). Constitutes the oldest formally defined unit in the Canning Basin [as of 2021]. Two new member subdivisions proposed although these are not consistently identified across all drilled intervals and not yet in seismic. Upper boundary was previously said to be where limestone becomes dominant; however, this approach was identified as flawed. Authors propose a sequence stratigraphic boundary definition instead (but also identify the boundary in HyLogger data as the first instance of ~100% carbonate). Underlain by Cambrian basement rocks. Part of supersequence A. Covers part of the J. gananda conodont biozone and the entirity of the P. proteus, P. opeki - S. bilobatus and O. communis biozones. Identified as a potential source rock but most data indicate low potential. More locations: p. 50-53, 55-56, 59-65, Pl.1-2, Pl.4.|ca 480 Ma-470 Ma||Samphire Marsh Member and Fly Flat Member|Conformably overlain by Willara Formation including Acacia Sandstone Member. Unconformably overlain by Grant Group. Equivalent to Wilson Cliffs Sandstone and Prices Creek Group (and units therein).||06-DEC-22
26070|Nambeet Formation|73345|5|Briefly described|p226-231|Floian|Tremadocian|Canning Basin. No longer the oldest identified formation in the basin (see Yapukarninjarra Formation). Constituents demonstrate (limited) potential for a CO2 storage reservoir/seal pair. Includes the J. gananda biozone.|||Samphire Marsh Member, Fly Flat Member|Conformably underlain by Yapukarninjarra Formation. Conformably overlain by Barnicarndy Formation.|Includes sandstone, siltstone and claystone.|
26070|Nambeet Formation|73346|6|Mentioned|p3, p27|Middle Ordovician|Early Ordovician|Canning Basin. Deposited in shallow marine environments. Upper portion may be age equivalent to Cobb Formation.||||Equivalent to Wilson Cliffs Sandstone.||
26070|Nambeet Formation|73567|5|Briefly described|p61-64, p66, p68-71|Floian|Tremadocian|Canning Basin. Good recovery in Olympic 1 petroleum well. Defined in the subsurface only. Six new high precision U-Pb (CA-ID-TIMS) ages are reported for bentonites throughout the upper portion of the unit ranging from 479.37 +/- 0.16 Ma to 471.32 +/- 0.11 Ma. New ages used to constrain four conodont biozones. [Includes reference to upper and lower subdivisions; see Fly Flat and Samphire Marsh members].|ca 480-473 Ma (see comments)|||Conformably overlain by Willara Formation. Equivalent to the Gap Creek and Emanuel formations (Prices Creek Group).|Includes black mudstone, limestone, and minor bentonite in the upper portion and dominantly sandstone in the lower portion.|
78698|Nambung Member|69788|3|Fully described|p1023-1024;p1027 Fig.3;p1029-1034;p1037|Pleistocene|Pleistocene|Defined. Name was erected informally by Hearty and O'Leary (2008). Type locality given. U/Th ages, Lipar and Webb, 2014. 5m to over 10m thick. Outcrops as pinnacles. Underwent karstification after deposition of eolianite; the dissolution voids were partly filled with laminated microbialites. Has a thick paleosol layer on top.|342 +/- 18 ka and 383 +/- 53 ka.|Unit in Tamala Limestone.||Overlies White Desert Member. Is overlain by Stockyard Gully Member or Pinnacles Desert Member. May correlate with Peppermint Grove Member.|Consists of an eolian calcarenite/calcrete-microbialite/paleosol cycle.|
78698|Nambung Member|69840|4|Described|p185, p187-188, p187 Tb.1, p196 Fig.13|Pleistocene|Pleistocene|See also p188 Fig.5, p190, p197, p198, p199. Dating using U/Th geochronology. Other dated sample: 0.342+/-0.018 Ma. Marine Isotope stage 10-11.|0.38300 +/- 0.05300 Ma|Tamala Limestone||Partially overlies White Desert Member and Tamala Limestone and partially underlies Stockyard Gully Member.|Generally consist of aeolian calcarenite (aeolianite),overlain by calcrete, microbialite and a palaeosol.|
77110|Nancar Sandstone|61548|6|Mentioned|p480 Fig.3|Early Cretaceous|Late Jurassic|Northern Bonaparte Basin.||||||
77110|Nancar Sandstone|68223|6|Mentioned|p178 Fig.3, p179 Fig.4|Tithonian|Tithonian|||||||
36770|Nandingarra Granodiorite|50381|5|Briefly described|Map Legend|Archean|Archean|Of Corunna Downs Granitoid Complex. Geological Province: Pilbara Craton. Age: 3313-3300 Ma||||||07-NOV-08
36770|Nandingarra Granodiorite|63441|5|Briefly described|p8 Tb. 2|Archean|Archean|Of Emu Pool Supersuite. Age: 3313+/-4Ma. Geological province: Pilbara Craton.||||||07-FEB-11
36770|Nandingarra Granodiorite|64327|5|Briefly described|p62, p63 Fig. 2|Archean|Archean|Forms an elliptical body of fine- to coarse-grained, equigranular, biotite granodiorite, with lesser tonalite and monzogranite; its eastern edge contains biotite tonalite to granodiorite with minor microcline.||||||07-NOV-08
36770|Nandingarra Granodiorite|64621|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite. Age: 3313-3300Ma.  Biotite-hornblende granodiorite to tonalite; equigranular; contains inclusions of Tambina Supersuite tonalite; metamorphosed.||||||07-NOV-08
36770|Nandingarra Granodiorite|65008|6|Mentioned|p12|||||Of the Corunna Downs Granitoid Complex||||
36770|Nandingarra Granodiorite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Emu Pool Supersuite. 3313-3300 Ma. Biotite-hornblende granodiorite to tonalite; equigranular; contains inclusions of Tambina Supersuite tonalite; weakly metamorphosed.||||||
36770|Nandingarra Granodiorite|69012|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane.|3313-3300 Ma|Of the Emu Pool Supersuite.|||Comprises biotite-hornblende granodiorite to tonalite; equigranular; contains inclusions of Tambina Supersuite tonalite; metamorphosed.|
36770|Nandingarra Granodiorite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Age derived from samples of biotite and biotite-hornblende tonalites (160211.1.pdf, 160212.1.pdf)|3313 Ma +/- 4 Ma - 3408 Ma +/- 7 Ma (SHRIMP)|Emu Pool Supersuite|||Biotite--hornblende granodiorite to tonalite; equigranular; contains inclusions of Tambina Supersuite tonalite; metamorphosed.|
36770|Nandingarra Granodiorite|69566|6|Mentioned|p236|||Corunna Downs Granitoid Complex, East Pilbara Granite-Greenstone Terrane.||||||
36770|Nandingarra Granodiorite|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA 160211 (altered biotite tonalite) yielded possible igneous crystallisation ages of 3408+\-7 Ma or 3427+\-4 Ma (both are weighted mean 207Pb/206Pb); if the c. 3427 Ma age does represent the igneous crystallisation age, then the c. 3408 Ma age would potentially represent indistinct veins or dykes, or a ragiogenic-Pb redistribution event. Likewise, if the c. 3408 Ma age represents the igneous crystallisation age, then the c. 3427 Ma age represent zircon xenocrysts. Sample GSWA 160212 (biotite-hornblende tonalite) yielded an interpreted igneous crystallisation age of 3313+\-4 Ma of the tonalite. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv.|3313-3300 Ma (isotopic)|Unit of Emu Pool Supersuite.|||Biotite-hornblende granodiorite to tonalite; equigranular; contains inclusions of Tambina Supersuite tonalite; metamorphosed|
36770|Nandingarra Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite, tonalite, monzogranite|
36770|Nandingarra Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||Max age 3313+/-3 Ma, min 3300+/-3 Ma.|Emu Pool Supersuite||Contains inclusions of Tambina Supersuite tonalite.|Biotite--hornblende granodiorite to tonalite; equigranular; contains inclusions of Tambina Supersuite tonalite; metamorphosed.|
80020|Nangetty Sequence|69297|6|Mentioned|p204, p223, p236|Sakmarian|Asselian|Offshore Perth Basin. Same diagram on three pages.||||Overlain by the Holmwood Sequence.||20-SEP-17
74818|Nannine Tonalite|64891|5|Briefly described|p37 Fig. 2, p38, p41, p50-51 Tb. 1|Archean|Archean|Of Cullculli Suite (Annean Supers'te). Age: c.2785Ma. Cross-cuts through Norie Gp. Geol.prov: Murchison Domain. Metatonalite, characterised by white-weathering appearance and an equigranular to weakly feldspar-porphyritic texture with 15-20% hornblende.||||||07-FEB-11
74818|Nannine Tonalite|69583|5|Briefly described|p52; Plate 2|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Appears as Nanine Tonalite on p52.||Cullculli Suite.|||Hornblende-bearing metagranodiorite.|
74818|Nannine Tonalite|70796|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Younami Terrane.|2785 +/ 5 Ma to 2780 +/ 5 Ma (isotopic)|Cullculli Suite|||Hornblendebearing metagranodiorite with minor metatonalite; contains scattered, small mafic xenoliths.|
74818|Nannine Tonalite|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv.|2787+\-3, 2782+\-7 Ma (isotopic)|Unit of Cullculli Suite.|||Hornblende metatonalite|
74818|Nannine Tonalite|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|2787-2782 Ma.|Cullculli Suite.|||Hornblende metatonalite.|
74818|Nannine Tonalite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Youanmi Terrane.|2787+/-3 Ma.|Cullculli Suite|||Hornblende metatonalite.|
36972|Nanular Member|23485|4|Described|p31|Mesoproterozoic|Paleoproterozoic|Of Ullawarra Formation.  Formerly Nanular Sandstone.||||||07-NOV-08
36972|Nanular Member|23487|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Ullawarra Formation. Geological Province: Edmund Basin.||||||07-NOV-08
36972|Nanular Member|65545|5|Briefly described|Map Legend|Mesoprotoerozoic|Paleoproterozoic|Of Ullwarra Formation, Edmund Basin. c. 1460 - <1620 Ma. Thin to thick bedded sandstone and siltstone.||||||
36972|Nanular Member|65549|5|Briefly described|Map Legend|Calymmian|Statherian|Of Ullawarra Formation (Edmund Group). Thin to thick-bedded sandstone and siltstone.||||||
36972|Nanular Member|65896|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Member of Ullawarra Formation in upper Edmund Group. Planar-laminated siltstone and thin- to medium-bedded quartz sandstone; thin lenses of pebble conglomerate.||||||
36972|Nanular Member|66112|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Member in Ullawarra Formation, Edmund Group. Thin- to thick-bedded sandstone and siltstone.||||||
36972|Nanular Member|69166|4|Described|geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|||Ullawarra Formation|||Thin- to thick-bedded sandstone and siltstone.|
36972|Nanular Member|70795|5|Briefly described|100k_geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Also 100k_interpgeop_lut.csv, West Australian Craton, Edmund Basin|1590-1455 Ma|Edmund Group|||Thin- to thick-bedded sandstone and siltstone.|
80997|Nanutarra Formation and Yarraloola Conglomerate|72034|5|Briefly described|500k_interpgeop16_lut|Aptian|Early Cretaceous|Northern Carnarvon Basin.  Informal combination of units for map scale. Age from biostratigraphy.|||||Poorly sorted sandstone (in places glauconitic), cobble to boulder conglomerate, and siltstone.|
27212|Napier Formation|7433|6|Mentioned|p53.|Devonian|Devonian|Lennard Shelf. Two "Mississippi Valley"-type lead-zinc orebodies were mined intermittently from 1906 to 1964.|||||Carbonates with Pb-Zn mineralisation.|
27212|Napier Formation|22550|6|Mentioned|Fig 3|||||||||
27212|Napier Formation|22741|5|Briefly described|P21, P23, Table3 P16||Devonian|Epuivalent to the Virgin Hills and Piker Hills Formations.||||||10-NOV-08
27212|Napier Formation|23722|4|Described|p32|Devonian|Devonian|Geological Province: Canning Basin.||||||13-NOV-07
27212|Napier Formation|24000|5|Briefly described|p348 Fig. 2|Famennian|Frasnian|Geological Province: Canning Basin.||||||
27212|Napier Formation|24061|5|Briefly described|p181|Late Devonian|Middle Devonian|Geological Province:  Canning Basin.||||||
27212|Napier Formation|24371|5|Briefly described|p206|Famennian|Frasnian|Reef maginal slope strata. Unconformably overlain by Nullara Formation and Windjana Limestone. Geological province: Canning Basin.||||||25-JAN-05
27212|Napier Formation|29845|6|Mentioned|p108|||||||||
27212|Napier Formation|30110|6|Mentioned|p81|||Upper Devonian,Frasnian - Famennian age.||||||
27212|Napier Formation|30181|6|Mentioned|p177|||||||||
27212|Napier Formation|30187|6|Mentioned|p179|||||||||
27212|Napier Formation|30525|6|Mentioned|Map legend|Famennian|Frasnian|Famennian to Frasnian||||||
27212|Napier Formation|30533|4|Described|p24|||On Table 6||||||
27212|Napier Formation|30896|4|Described|p19|||||||||
27212|Napier Formation|30897|4|Described|p18|||||||||
27212|Napier Formation|30898|6|Mentioned|Map legend|Famennian|Frasnian|Frasnian - Famennian||||||
27212|Napier Formation|31151|6|Mentioned|p69|||||||||
27212|Napier Formation|31152|6|Mentioned|Fig. 3|||||||||
27212|Napier Formation|31226|6|Mentioned|Map legend|Famennian|Frasnian|Frasnian to Famennian||||||
27212|Napier Formation|31332|6|Mentioned|Fig. 3|||||||||
27212|Napier Formation|31870|4|Described|p9|||See also Fig.14,15,17,18-21,23-26||||||
27212|Napier Formation|32141|6|Mentioned|p146|||||||||
27212|Napier Formation|32643|6|Mentioned|p535|||||||||
27212|Napier Formation|32647|6|Mentioned|p98|||||||||
27212|Napier Formation|32648|6|Mentioned|p32|||||||||
27212|Napier Formation|32865|6|Mentioned|p474|||See also P475. Fauna||||||
27212|Napier Formation|33042|6|Mentioned|p725|||||||||
27212|Napier Formation|33112|6|Mentioned|p179|||Devonian||||||
27212|Napier Formation|34427|6|Mentioned|Fig.3|||||||||
27212|Napier Formation|35104|6|Mentioned|p5|||||||||
27212|Napier Formation|36115|6|Mentioned|p133|||||||||
27212|Napier Formation|36225|6|Mentioned|Map legend|Famennian|Frasnian|Frasnian to Famennian||||||
27212|Napier Formation|36365|6|Mentioned|Fig.8|||||||||
27212|Napier Formation|36890|3|Fully described|p331|||||||||
27212|Napier Formation|38207|6|Mentioned|Fig.1|||||||||
27212|Napier Formation|38263|6|Mentioned|p16|||||||||
27212|Napier Formation|38274|6|Mentioned|p197|||||||||
27212|Napier Formation|38556|6|Mentioned|p56|||||||||
27212|Napier Formation|39702|6|Mentioned|Fig.2|||||||||
27212|Napier Formation|39796|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
27212|Napier Formation|40236|6|Mentioned|p132|||||||||
27212|Napier Formation|40793|6|Mentioned|p165|||||||||
27212|Napier Formation|40797|6|Mentioned|Fig.2|||||||||
27212|Napier Formation|40838|6|Mentioned|p280|||||||||
27212|Napier Formation|40901|6|Mentioned|p62|||||||||
27212|Napier Formation|41023|6|Mentioned|p288|||||||||
27212|Napier Formation|41139|6|Mentioned|Fig.2|||||||||
27212|Napier Formation|41158|6|Mentioned|p73|||See also P80 and Plate 2||||||
27212|Napier Formation|41169|6|Mentioned|Fig.3|||||||||
27212|Napier Formation|41492|6|Mentioned|Fig.10|||||||||
27212|Napier Formation|41828|6|Mentioned|Table 1|||||||||
27212|Napier Formation|41894|4|Described|p4|||||||||
27212|Napier Formation|41918|5|Briefly described|p103|||||||||
27212|Napier Formation|42030|5|Briefly described|p747|||||||||
27212|Napier Formation|42073|5|Briefly described|p291|||||||||
27212|Napier Formation|42111|6|Mentioned|Text fig.3 P90|||||||||
27212|Napier Formation|42347|5|Briefly described|Fig.4 P1021, Fig.2|Famennian|Frasnian|See also Fig.9 p1026.||||||13-NOV-07
27212|Napier Formation|42351|5|Briefly described|p45|||||||||
27212|Napier Formation|42564|5|Briefly described|p10|||See also Lower Napier Formation.||||||
27212|Napier Formation|42710|5|Briefly described|map legend|Late Devonian||||||||
27212|Napier Formation|42811|4|Described|p41|||see also Fig.9||||||
27212|Napier Formation|42814|5|Briefly described|p22|||||||||
27212|Napier Formation|42815|5|Briefly described|map|Late Devonian||||||||
27212|Napier Formation|42860|5|Briefly described|Fig.2|||||||||
27212|Napier Formation|42880|5|Briefly described|Fig.2,p1020|||||||||
27212|Napier Formation|42930|5|Briefly described|Fig.1 p473|Late Devonian|Devonian|Interfingers with Windjana Limestone. Geological Province: Canning Basin.||||||13-NOV-07
27212|Napier Formation|42933|5|Briefly described|Fig.94 p258|||||||||
27212|Napier Formation|42977|5|Briefly described|p274|||||||||
27212|Napier Formation|42994|6|Mentioned|p130|||||||||
27212|Napier Formation|43173|6|Mentioned|54||Late Devonian|||||||
27212|Napier Formation|43281|6|Mentioned|Map legend||Late Devonian|||||||
27212|Napier Formation|43563|6|Mentioned|Fig.5,p10||Late Devonian|||||||
27212|Napier Formation|43666|6|Mentioned|p14,47 Table 2||Famennian|||||||
27212|Napier Formation|43723|6|Mentioned|p51||Devonian|||||||
27212|Napier Formation|43815|6|Mentioned|Table 1,p95-96|||||||||
27212|Napier Formation|43818|6|Mentioned|p38|||||||||
27212|Napier Formation|44143|4|Described|p437 Table 4-19, p442, p443 Figure 4-98|Devonian|Devonian|Up to 1500m thick; calcarenite, calcirudite, and megabreccia; shallow marine. Interfingers with Windjana and Pillara Limestones. Type section along Barker River in Napier Range (LENNARD RIVER: 17deg 16' S, 124deg 44' E). Contains conodonts, goniatites, brachiopods and forams: early Frasnian to late Famennian.||||||23-NOV-17
27212|Napier Formation|44366|14|Not recorded|p.19, Table 3||Famennian|||||||
27212|Napier Formation|44367|14|Not recorded|map legend||Famennian|(Reprinted 1971).||||||
27212|Napier Formation|44397|14|Not recorded|p.11, Table 4||Famennian|||||||
27212|Napier Formation|44398|14|Not recorded|map legend||Famennian|||||||
27212|Napier Formation|44403|14|Not recorded|opp.p.6, Tb.1|||E/51-12. Correlates with Oscar Formation.||||||
27212|Napier Formation|44998|2|Defined|p41-43|||Overlies Pillara Formation. See also p26,27,36,45,50,54,60,249, App.3 p279.||||||
27212|Napier Formation|45063|6|Mentioned|p14|||See also Fig. 9. Dev.||||||
27212|Napier Formation|45101|6|Mentioned|p5|||See also P16, P22. Conodonts||||||
27212|Napier Formation|45133|6|Mentioned|Fig.3|||||||||
27212|Napier Formation|45143|3|Fully described|Fig.3|||Time-stratigraphic interpretations.||||||
27212|Napier Formation|45153|2|Defined|App.3-46|Late Devonian|Late Devonian|||||||
27212|Napier Formation|45158|3|Fully described|p24|||||||||
27212|Napier Formation|46869|6|Mentioned|Fig.1|||||||||
27212|Napier Formation|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
27212|Napier Formation|46994|6|Mentioned|p265|||||||||
27212|Napier Formation|47039|6|Mentioned|p133|||||||||
27212|Napier Formation|48848|14|Not recorded|p.36,37,39,62,65,69|||||||||
27212|Napier Formation|48931|5|Briefly described|p62|||||||||
27212|Napier Formation|50150|5|Briefly described|p280|Famennian|Famennian|See also p350 (ref: facing page). Geological Province: Canning Basin.||||||
27212|Napier Formation|64159|5|Briefly described|p91 Fig. 6|Famennian|Famennian|Part of the Lennard Reef facies development.||||||
27212|Napier Formation|64187|5|Briefly described|p320 Fig. 2|Frasnian|Frasnian|Formation is Fm in text. Underlain by Pillara Limestone, overlain unconformably by Virgin Hills Formation. Limestone, siltstone, sandstone (marine). Geological Province: Canning Basin.||||||01-MAY-13
27212|Napier Formation|64502|5|Briefly described|p764, p766 Fig.3, p785|Famennian|Givetian|Includes the Barrar, Tarakalu and Kalmanyi Members in the Dingo Gap area.||||||
27212|Napier Formation|64580|5|Briefly described|map legend|||Upper part: Famennian reef complexes, marginal slope and basin facies. Lower part: Givetian-Frasnian reef complexes, marginal slope and basin facies.||||||15-DEC-08
27212|Napier Formation|64643|5|Briefly described|p7 Fig. 5, p18|Famennian|Frasnian|Marginal slope deposits.||||||10-NOV-08
27212|Napier Formation|64981|6|Mentioned|p675.|||Mentioned as the point where Esso's Kora 1 drill terminated in 1982. Small quantities of oil were found in a sandy unit of the Betty Formation and gas from Nullara Limestone. Probable source was Laurel Formation.||||||
27212|Napier Formation|65486|5|Briefly described|p6-70, Plate 1.|Famennian|Frasnian|Reef complex, Canning Basin. Also referred to as Napier Limestone. Overlies Gogo Formation, Sadler Limestone, Pillara Limestone, underlies Virgin Hills Formation, Windjana Limestone.||||||
27212|Napier Formation|66127|3|Fully described|pp19-23, p62-64, p307-315, Pl. 2,3,6,7,8|Late Famennian|Early Frasnian|Name proposed by Guppy et al. (1958); current usage is that of Playford and Lowry (1966). Type section in Barker Gorge.  Includes all the exposed marginal-slope and basin facies rocks in the NW part of the Canning Basin reef complexes. Parts are equivalent to Virgin Hills, Piker Hills and Gogo Formations and Bugle Gap and Sadler Limestones. Map shows seven mapped units, three of which are named. Diverse fossil fauna. Rare leucite-lamproite diatreme vents. Frasnian and Famennian deposits are shown separately on the maps (Plates 3, 7).|||Includes Kalmanyi, Tarakalu and Barrar Members.|Interfingers with and abuts Windjana and Pillara Limestones.|Three units are mapped separately. Reef-slope and fore-reef facies: steeply-dipping limestone, some allochthonous blocks and debris flows, conglomerate, sandstone. Bioherms: deep water stromatolite and Receptaculites limestone.|
27212|Napier Formation|67131|6|Mentioned|p3 Fig. 2|Famennian|Givetian|Marginal slope and basin facies.||||||28-JAN-20
27212|Napier Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Famennian|Frasnian|Lennard Shelf. Canning Basin. Upper part: Famennian reef complexes, marginal slope and basin facies. Grouped as Piker Hills Formation, Bugle Gap Limestone, upper Napier Formation and upper Virgin Hills Formation. Lower part: Givetian-Frasnian reef complexes, marginal slope and basin facies. Grouped as Sadler Limestone, Gogo Formation, lower Virgin Hills Formation, and lower Napier Formation. Both groups used in 500k_geologyp08_lut.csv.|||||well-bedded to massive fore-reef, reefal slope, and basinal limestone; locally dolomitized and steeply dipping; locally microbial and sponge rich; some allochthonous blocks and debris flows, some sandstone|
27212|Napier Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Famennian|Famennian|||||||
27212|Napier Formation|69634|4|Described|250k_interpgeop_lut.csv|Famennian|Frasnian|Of Lennard Shelf, Canning Basin. Frasnian-Famennian reef complexes, marginal slope and basinal facies. Events: Alice Springs Orogeny.|382.7-358.9 Ma (biostrat)||||Well-bedded to massive fore-reef, reefal slope, and basinal limestone; locally dolomitized and steeply dipping; locally microbial and sponge rich; some allochthonous blocks and debris flows, some sandstone|
27212|Napier Formation|69660|5|Briefly described|Map legend|Famennian|Frasnian|Canning Basin.|||||Well-bedded to massive fore-reef, reefal-slope and basinal limestone; locally dolomitized and steeply dipping; locally microbial and sponge-rich; some allochthonous blocks and debris flows, some sandstone (section only).|
27212|Napier Formation|70126|5|Briefly described|Map legend|Famennian|Frasnian|Canning Basin. Devonian Reef Complex.|||||Well-bedded to massive fore-reef, reefal slope, and basinal limestone; locally dolomitized and steeply dipping; locally microbial and sponge-rich; some allochthonous blocks and debris flows, some sandstone.|
27212|Napier Formation|70154|4|Described|100k_geologyp_lut.csv|Famennian|Frasnian|See also 100k_geologyp_lut.csv.|359-383 Ma||||Well-bedded to massive fore-reef, reefal slope, and basinal limestone; locally dolomitized and steeply dipping; locally microbial and sponge rich; some allochthonous blocks and debris flows, some sandstone.|
27212|Napier Formation|70492|6|Mentioned|p173|||Canning Basin.||||Is overlain by Fairfield Group.|Includes intraclastic breccia facies.|
27212|Napier Formation|71146|6|Mentioned|p31 fig 25|Upper Devonian|Devonian|Northern Canning Basin. Deposited in fore-reef subfacies.||||||
27212|Napier Formation|71267|4|Described|GEOL_LUT_CSV files|Famennian|Frasnian|Of Lennard Shelf, Canning Basin. Devonian reef complex. Events: Meda Transpression (323-310 Ma); Red Bluffs Extension (372.2-360 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma); Pillara Movement (Alice Springs Orogeny phase 2) (390-360 Ma); Van Emmerick Extension (382.7-372.2 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyp_lut.csv.|382.7-362 Ma (biostrat)||||Well-bedded to massive fore-reef, reefal slope, and basinal limestone; locally dolomitized and steeply dipping; locally microbial and sponge rich; some allochthonous blocks and debris flows, some sandstone|
27212|Napier Formation|71892|6|Mentioned|p10|Famennian|Frasnian|||||||
27212|Napier Formation|72502|6|Mentioned|p3, p5|Famennian|Givetian|Lennard Shelf and Fitzroy Trough, Canning Basin.||||Equivalent to Piker Hills Formation, Virgin Hills Formation, Gogo Formation, and Cadjebut Formation.||
32581|Nardoo Granite|22904|4|Described|p58|Orosirian|Orosirian|Age 2005-1985 Ma ie Palaeoproterozoic.||||||16-JUL-08
32581|Nardoo Granite|23485|4|Described|p19|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
32581|Nardoo Granite|23486|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Dalgaringa Supersuite. Geological Province: Gascoyne Complex.||||||07-NOV-08
32581|Nardoo Granite|23525|4|Described|p17|Orosirian|Orosirian|Age: c.1975Ma||||||
32581|Nardoo Granite|23527|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Dalgaringa Supersuite, Gascoyne Complex||||||07-NOV-08
32581|Nardoo Granite|23781|5|Briefly described|p48|Paleoproterozoic|Paleoproterozoic|Age: c.1975Ma.||||||07-NOV-08
32581|Nardoo Granite|24544|4|Described|p10 Tb.1, p31|Paleoproterozoic|Paleoproterozoic|Age: c. 1975 Ma. Of Dalgaringa Supersuite. Porphyritic biotite tonalite and granodiorite.||||||07-NOV-08
32581|Nardoo Granite|50216|5|Briefly described|p212|Paleoproterozoic|Paleoproterozoic|Age: ca. 1975 Ma.||||||07-NOV-08
32581|Nardoo Granite|50218|5|Briefly described|p240 Fig.2, p247|Orosirian|Orosirian|Of the Dalgaringa Supersuite. Age: c.1975Ma. Geological Province: Glenburgh Terrane (Gascoyne Complex).||||||07-FEB-11
32581|Nardoo Granite|50219|4|Described|p260 Fig. 2, p263|Orosirian|Orosirian|Of the Dalgaringa Supersuite. Tonalite and granodiorite plutons. Age: c.1975Ma.  Geological Province: Glenburgh Terrane (Gascoyne Complex).  See also p268, p272.||||||07-FEB-11
32581|Nardoo Granite|50220|5|Briefly described|p280, p292 Tb.2|Orosirian|Orosirian|Age: c.1975 Ma.||||||
32581|Nardoo Granite|63866|5|Briefly described|p156-p157|Orosirian|Orosirian|Numeric ages are derived from Nelson, 1999 and are U-Pb SHRIMP dates.|1977 +/- 4 Ma and 1974 +/- 4 Ma|||Intrudes the Dalgaringa Supersuite.||
32581|Nardoo Granite|65692|5|Briefly described|p25, p30, p35|Orosirian|Orosirian|Intrudes the southern Glenburgh Terrane. Similar in age to, and thus possible source of, the youngest (1971 +/- 26 Ma) detrital zircon in the Yelma Formation (Earaheedy Basin).|c.1975 Ma.|||||06-MAR-17
32581|Nardoo Granite|66002|6|Mentioned|p6 Tb.5|||Used by Bibby and Moore (1998). Superseded name for Grieves Granite ||||||
32581|Nardoo Granite|66299|4|Described|p4 Fig.2, pp73-84, p162.|Paleoproterozoic|Paleoproterozoic|Component of Glenburgh Terrane, basement to Gascoyne Province. Equivalent to the gneissic biotite-hornblende granodiorite of the informally-named Dalgety Gneiss Dome of Williams (1986). Contains rafts of calc-silicate gneiss from Moogie Metamorphics.|c.1975 Ma.|Unit in Dalgaringa Supersuite.||Intrudes older units- foliated and gneissic granites- of Dalgaringa Supersuite. Intruded by Moorarie Supersuite dykes.|Foliated, medium-grained biotite metatonalite, metagranodiorite and metamorphosed quartz-diorite; equigranular or porphyritic; abundant small mafic clots.|
32581|Nardoo Granite|66427|6|Mentioned|p40 Fig.1|||Glenburgh Terrane. Appears as Nardoo granite.|1.97 Ga.|||||
32581|Nardoo Granite|66887|5|Briefly described|p3 Fig.2, p5 Fig.4|Orosirian|Orosirian|Glenburgh Terrane, southern Gascoyne Province.|~1975 Ma estimated from Fig.4.|Dalgaringa Supersuite||||
32581|Nardoo Granite|66950|6|Mentioned|p9 Fig.8|Orosirian|Orosirian||c. 2000-1900 Ma|||||
32581|Nardoo Granite|67247|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, Gascoyne Province.|2002 - 1974 Ma.|Unit in Dalgaringa Supersuite.|||Foliated, medium-grained biotite metatonalite and meta quartz diorite; equigranular or porphyritic; abundant small mafic clots.|
32581|Nardoo Granite|67371|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, Gascoyne Province.||Unit in Dalgaringa Supersuite.|||Foliated, medium-grained biotite metatonalite and meta quartz diorite; equigranular or porphyritic; abundant small mafic clots; local foliated leucocratic biotite metamonzogranite, commonly with clots of biotite after garnet.|
32581|Nardoo Granite|67843|4|Described|p2 Fig.1, p4, p11, p38.|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane. Deformation and mineralogy are described in some detail.|1979-1974 Ma.|Unit in Dalgaringa Supersuite.||Intrudes Dalgaringa Supersuite.||
32581|Nardoo Granite|69080|5|Briefly described|p686 Fig.4, p696|Orosirian|Orosirian|Gascoyne Province.|c.1980 Ma.|Unit in Dalgaringa Supersuite.||||
32581|Nardoo Granite|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Age derived from biotite tonalite sample (142928.1.pdf)|1974 Ma +/- 4 Ma (SHRIMP)|Dalgaringa Supersuite|||Foliated, medium-grained, weakly porphyritic, leucocratic biotite metatonalite and minor metagranodiorite|
32581|Nardoo Granite|69387|5|Briefly described|p3, p6, p12, p21, p26-28, p35|Orosirian|Orosirian|Deformations discussed. SG and magnetic susceptibility values given. Gravity and magnetic modelling. Petrophysically distinct.|c.1980-1970 Ma (Occhipinti et al., 2004).|Dalgaringa Supersuite.|||Relatively undeformed post-tectonic stocks and plutons of arc-related granite.|
32581|Nardoo Granite|69596|6|Mentioned|p5|Orosirian|Orosirian|Gascoyne Province.||||||
32581|Nardoo Granite|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_interpgeop_lut.csv, 142928.1.pdf, 142929.1.pdf, 142932.1.pdf|1977-1974 Ma||||Foliated, medium grained biotite metatonalite and metamorphosed quartz diorite. Foliated, medium grained, weakly porphyritic leucocratic biotite metatonalite and minor metagranodiorite. Biotite monzogranite, biotite tonalite, granodiorite.|17-AUG-22
32581|Nardoo Granite|70814|6|Mentioned|p62|||||||||
32581|Nardoo Granite|71000|6|Mentioned|p65|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, southern Gascoyne Province, Capricorn Orogen.||||||
32581|Nardoo Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||tonalite, quartz diorite, granodiorite|
32581|Nardoo Granite|71269|4|Described|1m_geologyp12_lut.csv|||Geological province: Gascoyne Province, Glenburgh Terrane, Capricorn Orogen, West Australian Craton.|||||Foliated, equigranular to porphyritic, medium grained biotite tonalite and quartz diorite, with abundant small mafic clots; minor leucocratic tonalite and granodiorite.|
32581|Nardoo Granite|71869|5|Briefly described|p3, p5, p9, p12, p17, app p4-p5|||Glenburgh Terrane, Capricorn Orogen.||Dalgaringa Supersuite|||Porphyritic granodiorite, biotite tonalite and mesocratic tonalite.|
32581|Nardoo Granite|72259|6|Mentioned|App. Tb.B||||||||Includes porphyritic granodiorite.|
32581|Nardoo Granite|73168|6|Mentioned|p758|||Glenburgh Terrane.||Dalaringa Supersuite||||
32581|Nardoo Granite|73214|5|Briefly described|p974 Fig.1|Palaeoproterozoic|Palaeoproterozoic|Glenburgh Terrane.||Dalgaringa Supersuite||||
76821|Nargalyerin Soak Monzogranite|69559|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|See also geologyp_lut.csv, 500k_interpgeop_lut.csv..|2637-2632 Ma||||Medium grained biotite monzogranite; metamorphosed.|
76821|Nargalyerin Soak Monzogranite|70156|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|2637+\-5 Ma; 263+\7 Ma (isotopic)||||Medium-grained biotite monzogranite; metamorphosed|
76821|Nargalyerin Soak Monzogranite|70204|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton.|2639-2632 Ma.||||Medium-grained biotite monzogranite; metamorphosed.|
76821|Nargalyerin Soak Monzogranite|70794|5|Briefly described|500k_interpgeop_lut.csv|Neoarchean|Neoarchean|Also 100k_interpgeop_lut.csv, 100k_geologyp_lut.csv.|2632 +/-7Ma-2637+/-5 Ma||||Medium grained biotite monzogranite; metamorphosed.|
82173|Narilya Bore Basalt|73084|4|Described|p: 23, 27, 74-82, 90-91, 119-124...|Ectasian|Calymmian|Madura Province. Occurs as inclusions within the Kestrel Cavern Gabbro, although a genetic relationship is unlikely based on significantly different geochemical signatures. Buried and deformed before intrusion of the Kestrel Cavern Gabbro. Possibly up to granulite facies metamorphism related to intrusion of the Kestrel Cavern Gabbro. Formed distal to the continental margin in a subduction-related setting similar to but more distal than that of the Sleeper Camp Formation and Malcolm Metamorphics. Report includes lithologic/petrographic description, whole-rock geochemistry, Sm-Nd. Also p: 127, 130, 132, 140-141.|c. 1400 Ma|||Intruded by Kestrel Cavern Gabbro.|Fine-grained (average 1-2 mm), layered to laminated, locally foliated mafic rock.|
73261|Narimbunna Dolerite|63469|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Dolerite and gabbro sills intruding the Edmund Group. Age dated at c.1465Ma.||||||07-NOV-08
73261|Narimbunna Dolerite|63470|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age: c. 1465Ma. Dolerite and gabbro sills intruded into the Edmund Group.||||||
73261|Narimbunna Dolerite|63471|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Within the Bangemall Supergroup. Comprises dolerite and gabbro sills which intrude into the Edmund Group.||||||12-SEP-07
73261|Narimbunna Dolerite|64580|4|Described|map legend||Mesoproterozoic|Dolerite and gabbro sills intruded into Edmund Group.||||||15-DEC-08
73261|Narimbunna Dolerite|65450|5|Briefly described|p4-6, 27|||Broadly conformable sills intrude Kiangi Creek Formation, although one thicker discordant vein is low angled. Au mineralisation.|1465 Ma sills.|||Sills intrude Kiangi Creek Formation.|Finely disseminated gold found in thin veins of cellular to massive variscite.|
73261|Narimbunna Dolerite|65453|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Dolerite and gabbro sills intruded into Edmund Group. Age: c. 1465 Ma.||||||
73261|Narimbunna Dolerite|65506|6|Mentioned|p987-988||~1465 Ma.|||||||
73261|Narimbunna Dolerite|65545|5|Briefly described|Map Legend|Mesoprotoerozoic|Paleoproterozoic|c. 1465 Ma. Dolerite and Gabbro sills intruded into Edmund Group.||||||
73261|Narimbunna Dolerite|65549|5|Briefly described|Map Legend|Calymmian|Calymmian|Dolerite and gabbro sills intruded into Edmund Group. Age of c. 1465 Ma given. Excluded from Bangemall Supergroup.||||||11-JUN-14
73261|Narimbunna Dolerite|66104|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Dolerite and gabbro sills intruded into Edmund Group, age shown as c. 1465 Ma.||||||
73261|Narimbunna Dolerite|66105|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Dolerite and gabbro sills intruded into Edmund Group. Age: c.1465 Ma.||||||
73261|Narimbunna Dolerite|66110|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age c.1465 Ma. Amphibolite; dolerite and gabbro sills intruded into Edmund Group.||||||
73261|Narimbunna Dolerite|66112|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Unit in Bangemall Supergroup. Aged c.1465 Ma. Dolerite and gabbro sills intruded into Edmund Group.||||||
73261|Narimbunna Dolerite|66241|5|Briefly described|pp1-4, p9. |Calymmian|Calymmian||c.1465 Ma.|||Intrudes Edmund Group.||
73261|Narimbunna Dolerite|66299|4|Described|p6 Fig.3, p299, p309.|Mesoproterozoic|Mesoproterozoic|Gascoyne Province. Also called Narimbunna Dolerite Sills on p.299. Strongly foliated.|c.1465 Ma.|||Intrudes Dingo Creek Granite and Edmund Group.|Amphibolite; most are fine-grained rocks with a polygonal texture, comprising hornblende, plagioclase, quartz and titanomagnetite.|
73261|Narimbunna Dolerite|66887|5|Briefly described|p5 Fig.4|Mesoproterozoic|Mesoproterozoic|Southern Gascoyne Province.|~1460 Ma estimated from Fig.4.|||||
73261|Narimbunna Dolerite|66950|6|Mentioned|p9 Fig.8|Calymmian|Calymmian||c. 1500-1400 Ma|||||
73261|Narimbunna Dolerite|67136|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||c.1465 Ma.|||Intrudes Edmund Group.|Dolerite and gabbro sills intruded into Edmund Group.|14-NOV-11
73261|Narimbunna Dolerite|67245|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||c.1465 Ma.|Unit in Bangemall Supersuite.||Intrudes several units of the Edmund Group.|Dolerite and gabbro sills intruded into Edmund Group.|
73261|Narimbunna Dolerite|67246|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||c.1465 Ma.|Unit in Bangemall Supergroup.||Intrudes several Formations in Edmund Group.|Dolerite and gabbro sills intruded into Edmund Group.|
73261|Narimbunna Dolerite|67247|6|Mentioned|Map legend.|||Shown only in Interpreted bedrock geology map legend. Not included in Bangemall Supergroup.||||||20-NOV-13
73261|Narimbunna Dolerite|67346|5|Briefly described|p795 Fig.2, p796 Fig.3|Calymmian|Calymmian||1465 Ma|||Intrudes Kiangi Creek Formation||11-MAY-12
73261|Narimbunna Dolerite|67374|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||c.1465 Ma.|Unit in Bangemall Supergroup.||Intrudes Edmund Group.|Dolerite and gabbro sills.|
73261|Narimbunna Dolerite|68285|5|Briefly described|Map Legend|Calymmian|Calymmian||c. 1465 Ma|||Intrudes into the Edmund Group.|Dolerite and gabbro sills.|
73261|Narimbunna Dolerite|68286|5|Briefly described|Map Legend|Calymmian|Calymmian||c. 1465 Ma|||Intrudes into the Edmund Group.|Dolerite and gabbro sills.|
73261|Narimbunna Dolerite|68521|5|Briefly described|Map Legend|Calymmian|Calymmian||c.1465 Ma|||Intrudes into the Edmund Group.|Dolerite and gabbro sills.|
73261|Narimbunna Dolerite|68522|5|Briefly described|Map Legend|Calymmian|Calymmian||c.1465 Ma|||Intrudes into the Edmund Group.|Dolerite and gabbro sills.|
73261|Narimbunna Dolerite|68981|5|Briefly described|p25-26|Calymmian|Calymmian|Appears as Narimbunna Dolerites on p26.|c.1465 Ma (Martin and Thorne, 2004).|||Intrudes Edmund Group.|Voluminous mafic sills.|
73261|Narimbunna Dolerite|69003|5|Briefly described|p4, p34-35|||Capricorn Orogen. These intrusions mark the end of Edmund Group period of sedimentation and extension.|1500-1465 Ma.|||Intrudes Ullawarra Formation (Edmund Group).|Voluminous mafic sills.|
73261|Narimbunna Dolerite|69028|5|Briefly described|Map Legend|Calymmian|Calymmian||c. 1465 Ma|||Intrudes the Edmund Group.|Dolerite and gabbro sills.|06-MAY-14
73261|Narimbunna Dolerite|69080|5|Briefly described|p684, p698|Calymmian|Calymmian|Gascoyne Province.|c.1465 Ma.||||Dolerite and gabbro sills intruded into Edmund Group.|
73261|Narimbunna Dolerite|69166|4|Described|geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|||||Intrudes into Edmund Group|Dolerite and gabbro sills; Amphibolite.|
73261|Narimbunna Dolerite|69185|4|Described|500k_geologyp08_lut.csv||Mesoproterozoic|Geological Province: Pilbara Craton.|||||Dolerite and gabbro sills intruded into Edmund Group|
73261|Narimbunna Dolerite|69387|5|Briefly described|p7, p22-34, p50|Calymmian|Calymmian|Prominent sills intruding the Edmund Basin, and visible in aeromagnetic and gravity data. SG and magnetic susceptibility values given. Appears as Narimbunna Dolerite Suite on p23-24. Gravity and magnetic modelling.|c.1465 Ma.|||Intrudes Edmund Group.|Voluminous mafic sills.|
73261|Narimbunna Dolerite|69554|6|Mentioned|p140|||Intrudes the Capricorn Orogen. Hf isotopes indicate a source extracted from the mantle at c.1950-1900 Ma.|c.1465 Ma.|||||
73261|Narimbunna Dolerite|69596|6|Mentioned|p4-5, p12-13|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.|c.1515-1465 Ma (Wingate, 2002).|||||
73261|Narimbunna Dolerite|70019|6|Mentioned|p93-94|Calymmian|Calymmian|Geological province: Gascoyne Province, Capricorn Orogen. Intrusion within the Edmund Group at different stratigrasphic levels; within Ullawarra Formation and uppermost Kiangi Formation.|c. 1465 Ma|||||
73261|Narimbunna Dolerite|70127|5|Briefly described|Map legend|Calymmian|Calymmian||1465-1449 Ma.||||Dolerite and gabbro sills intruded into Edmund Group.|
73261|Narimbunna Dolerite|70138|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||c.1465 Ma.||||Dolerite and gabbro sills intruded into Edmund Group.|
73261|Narimbunna Dolerite|70795|5|Briefly described|100k_geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Also 2_5m_interpgeop15_lut.csv, 100k_geologyl_lut.csv, 100k_interpgeop_lut.csv, 143445.1.pdf, 206991.1.pdf, West Australian Craton, Edmund Basin|1465-1449 Ma|||Intrudes into Edmund Group|Amphibolite. Dolerite and gabbro sills.|
73261|Narimbunna Dolerite|70814|5|Briefly described|p3, p5, p22, p34, p36-p37, p47-p48|Calymmian|Calymmian|Edmund Basin. |1465-1452 Ma (Wingate, 2002; Martin et al., 2005)|||Intrudes the Edmund Group.||
73261|Narimbunna Dolerite|70826|6|Mentioned|p10|Mesoproterozoic|Mesoproterozoic|||||Intrudes the Edmund Group. Broadly coeval with Warlawurru Supersuite in Musgrave province..||20-MAY-20
73261|Narimbunna Dolerite|71042|6|Mentioned|p96|||||||||
73261|Narimbunna Dolerite|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||dolerite, gabbro|
73261|Narimbunna Dolerite|71273|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||1465-1449 Ma.|||Intrudes Edmund Group.|Dolerite and gabbro sills intruded into Edmund Group.|
73261|Narimbunna Dolerite|71484|5|Briefly described|p125|||Geological province: Of Edmund and Collier basins. Intruded into Edmund Group.|||||Dolerite and gabbro sills.|30-AUG-19
73261|Narimbunna Dolerite|71869|6|Mentioned|p4|||Actually listed as Narimbunna Dolerite Suite, along with Waldburg Dolerite Suite.|c. 1450-1500 Ma|||||20-MAY-20
73261|Narimbunna Dolerite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Edmund Basin. |Max age 1465+/-3 Ma, min 1449+/-5 Ma.|||Sills intruded into Edmund Group.|Dolerite and gabbro sills intruded into Edmund Group.|
73261|Narimbunna Dolerite|72259|6|Mentioned|p3|Calymmian|Calymmian||ca. 1465 Ma|||||
73261|Narimbunna Dolerite|72705|5|Briefly described|p4||||c.1455 Ma.|||Intrudes (cross-cuts) Edmund Group.|Dolerite.|
73261|Narimbunna Dolerite|73102|4|Described|p: 1-4, 5, 6-8, 12, 17-20, 22, 28, 31|Calymmian|Calymmian|Gascoyne Province. Forms extensive dolerite sills within sedimentary rocks of the Edmund Basin, but not  Collier Basin. Sills are highly altered and similar in mineralogy to Minga [Dolerite] dykes; however, are geochemically and petrogenetically distinct, and are not spatially associated. Sills formed through remelting of a previously subduction-modified mantle source, and underwent more or less closed-system compositional evolution during emplacement.|1465-1450 Ma|||Intruded by Mundine Well Dolerite. Intrudes Edmund Group.|Dolerite and gabbro sillsintruded into Edmund Group.|
73261|Narimbunna Dolerite|73442|4|Described|p1-3, p5-6, p9-20, p23-27, p35-38, p40|Calymmian|Calymmian|Capricorn Orogen, western. Weighted mean age of 1450+/-3 Ma from four samples, an older age of 1465+/-3 Ma may represent a separate episode of dolerite intrusion. Emplaced only within the Edmund Basin, occurs in all stratigraphic levels below the Coodardoo Formation. Most sills are locally conformable with bedding, they are regionally discordant along strike and locally step upwards through stratigraphy. Maximum composite thickness of sills is about 1000m, thickness reduces towards the east. Characterised mostly as a high-Fe tholeiitic basalt. Location in text includes iii-iv.|1465-1449 Ma U-Pb SHRIMP zircon and baddeleyite|||Intruded into Edmund Group|Dolerite and gabbro sills, locally exhibits igneous layering or foliation, and irregular enclaves or veins of very coarse-grained to pegmatitic leucogabbro. Typically moderately to strongly altered.|
74876|Narndee Igneous Complex|64891|5|Briefly described|p37 Fig. 2, p44, p50-51 Tb. 1|Archean|Archean|Of the Boodanoo Suite. Age: 2780Ma. Geological province: Murchison Domain. Mafic-ultramafic suite dominated by hornblende gabbros: layered gabbro, with dunite, pyroxenite, anorthosite, and hornblende gabbro; includes younger leucogabbro; metamorphosed||||||07-FEB-11
74876|Narndee Igneous Complex|66195|4|Described|p604, 601, 2,6,8, 597,598,p599 Fig.2|Neoarchean|Mesoarchean|Yilgarn Craton. Divided into ultramafic zone ~2km thick, lower zone ~1km thick and the main zone ~2km thick. See figure 4 p602 for more detail. New zircons and baddeleyite crystallisation age. More ultramafics and hornblende gabbro than Meeline Suite units.|Crystallisation age of 2800 +/- 6 Ma.|In Boodanoo Suite.||Intrudes Norie Group.||13-MAR-12
74876|Narndee Igneous Complex|67129|6|Mentioned|vi, p18, p20, p51-57, p59-61, p64-65|Archean|Archean|Murchison Domain, Youanmi Terrane. Exposed over 30km N-S and 25km E-W. 4.5 km thick. Coeval with Norie Group eruptions.|2800 +/- 6 Ma.|Boodanoo Suite|||Ultramafics, leucogabbro sheets, gabbronorite, peridotite and pyroxenite, hornblende gabbro.|07-SEP-17
74876|Narndee Igneous Complex|68109|6|Mentioned|p659|||Youanmi Terrane. ||||Contemporaneous with the Norie Group and Windimurra Igneous Complex.|Large layered mafic-ultramafic igneous complex.|
74876|Narndee Igneous Complex|68110|5|Briefly described|p673, p686-687|Mesoarchean|Mesoarchean|~ 170 km south-southeast of Cue. At least 700 km2. Members contain substantial hydrous phases (hornblende, phlogopite); have boninite-like light REE enriched patterns.|ca. 2800 Ma|Of the Boodanoo Suite.||||
74876|Narndee Igneous Complex|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane.  Gabbronorite U-Pb zircon age: 2799 +/- 7 Ma igneous crystallization age. See geochron file 191056.1.pdf.||Boodanoo Suite|Includes 33 unnamed subunits in Middle, Lower and Ultramafic zones.||Sepentinite; Metagabbro; Dolerite; gabbronorite; schist; pyroxenite; Anorthosite; Leucogabbronorite; Troctolite; Leuconorite; Metagabbronorite; Gabbronorite; Metadunite; Ultramafic schist; Pyroxene peridotite.|
74876|Narndee Igneous Complex|68698|5|Briefly described|p5|Neoarchean|Mesoarchean|Up to 7km thick and 80km diameter.|c.2800 Ma (Ivanic et al., 2010).||||Very large layered mafic-ultramafic igneous complex.|
74876|Narndee Igneous Complex|69404|6|Mentioned|p2|||Synchronously emplaced with the Windimurra Igneous Complex and the Norie Group.|||||Mafic to ultramafic rocks.|
74876|Narndee Igneous Complex|69583|4|Described|p47, p49-50, p55-56, p98-102, p110, p116|Neoarchean|Mesoarchean|See also p177; Plate 2. Murchison Domain, western Youanmi Terrane; south of the Windimurra Igneous Complex. Constitutes the Boodanoo Suite. Emplacement was accompanied by Norie Group volcanism. Another age determination is a Sm-Nd whole-rock isochron age of 2824 +/- 80 Ma (Scowen, 1991). Mineralisation style, geochronological data, igneous stratigraphic column. The Middle, Lower and Ultramafic Zones are mapped separately in Plate 2.|2800 +/- 6 Ma (Ivanovic et al., 2010).|Boodanoo Suite.||Intrudes the Norie Group.|Layered mafic-ultramafic igneous complex. Compositionally distinctive: contains a large volume of hornblende gabbro, a larger proportion of ultramafic rocks, and lacks the characteristic magnetite layers of Meeline Suite intrusives.|
74876|Narndee Igneous Complex|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean|||Boodanoo Suite||||
74876|Narndee Igneous Complex|69586|5|Briefly described|p18, p22-23|Neoarchean|Mesoarchean|||Boodanoo Suite.||||
74876|Narndee Igneous Complex|69617|6|Mentioned|p154|||Murchison Domain, Youanmi Terrane.|c.2800 Ma.|||||
74876|Narndee Igneous Complex|69626|5|Briefly described|map legend|Archean|Archean|Informal Middle zone, Lower zone and Ultramafic zone contain multiple unnamed units. Additional unnamed units are also listed. Detailed lithology in legend. Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Boodanoo Suite|||Layered mafic/ultramafic igneous rocks. Middle zone: interlayered gabbronorite - serpentinite; leucogabbronorite. Lower zone: interlayered gabbronorite - pyroxenite - peridotite. Ultramafic zone: interlayered pyroxene peridotite - olivine pyroxenite.|
74876|Narndee Igneous Complex|70332|5|Briefly described|p76-84|Archean|Archean|Central Youanmi Terrane, Yilgarn Craton. Appears as NIC after first one or two mentions in text. Extends 29 km in diameter. This age is consistent with a new plateau age of 2805 +/- 14 Ma (hornblende 40Ar/39Ar). Crustal assimilation is ruled out as the source of water in the magma; three alternative scenarios are discussed.|2800 +/- 6 Ma (SIMS U-Pb; Ivanic et al., 2010).||||Large layered mafic-ultramafic intrusion, notable for presence of crystal-bound water (abundant hornblende). Large parts metamorphosed to greenschist or lower amphibolite facies.|
74876|Narndee Igneous Complex|70419|5|Briefly described|p2, p7-9, p11, p24|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Lacks the distinctive magnetitite units in the upper zone that characterise the Meeline Suite igneous complexes.|2800 Ma.|Boodanoo Suite.||||
74876|Narndee Igneous Complex|70770|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Divided into three zones: ultramafic, lower (eleven facies) and middle (eight facies), and a metagabbro unit; all 21 units are mapped separately.|c.2800 Ma.|Boodanoo Suite.|||Pyroxene peridotite grading into orthopyroxenite; chromitite; serpentinite; gabbronorite; troctolite; metagabbronorite and metagabbro; schistose amphibolite; hornblende gabbro.|
74876|Narndee Igneous Complex|70796|5|Briefly described|100k_interpgeol_lut.csv,|Mesoarchean|Mesoarchean| Yilgarn Craton, Youanmi Terrane. See also 100k_interpgeop_lut.csv,  500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, site_lithology.csv, 185995.1.pdf, 191056.1.pdf, Bungar100_2539_stratig.pdf, Coolamaninu100_2540_stratig.pdf.. Informally subdivided into a middle and lower zone. Appears as Narndee Complex in site_lithology.csv.|ca 2800 Ma (inferred)||||Anorthosite, troctolite, leucogabbronorite, serpentinite, coarse pyroxenite, minor gabbronorite, chromitite. Metagabbro with rafts of psammite, pelite and quartzite, metadolerite. Tremolitechloritetalc schist.|
74876|Narndee Igneous Complex|70830|4|Described|p3-p4, p27, p29, p48-p55|Neoarchean|Mesoarchean|Sm-Nd age is derived from Scowen, 1991.|2824 +/- 80 Ma (Sm-Nd whole-rock)|||Intrudes the Norie Group.|Hornblende gabbro and extensive ultramafic rocks.|
74876|Narndee Igneous Complex|71168|4|Described|p7-p8, p18, p21-p22, p60|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c. 2800 Ma|Boodanoo Suite||Overlain by the Kantie Murdana Volcanics Member and the Norie Group.|Layered mafic-ultramafic rocks.|
74876|Narndee Igneous Complex|71311|6|Mentioned|p794|||Northern Youanmi Terrane, Yilgarn Craton.||||||
74876|Narndee Igneous Complex|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Mesoarchean|Youanmi Terrane. Lower: Gabbronorite interlayered with pyroxenite; local interstitial hornblende; metamorphosed. Middle: Megacycles of serpentinite grading into pyroxenite, gabbronorite, and anorthosite; typically with hornblende-oikocrystic units; gabbroic rocks dominant; metamorphosed. Ultramafic: Pyroxene peridotite interlayered with olivine pyroxenite grading into orthopyroxenite; minor hornblende typically as oikocrysts around pyroxene; typically serpentinized; locally strongly sheared.||Boodanoo Suite|Informally subdivided into lower, middle and ultramafic zones.||Layered gabbro, with dunite, pyroxenite, anorthosite, and hornblende gabbro; local well developed cyclical layering on a hundred metre scale; metamorphosed.|
74876|Narndee Igneous Complex|73596|6|Mentioned|p1161, 1170, 1172|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane.|2799 +/- 7 Ma.|Polelle Group.|||Includes sanukitoids and hydrous mafic intrusions.|
26072|Nathan Group|14019|6|Mentioned|p14|||Possibly correlates with sedimentary units in the Victoria Basin.  Geological Province: McArthur Basin.||||||
26072|Nathan Group|22453|6|Mentioned|p 12|||McArthur Basin||||||
26072|Nathan Group|22479|5|Briefly described|fig4, pg10|Calymmian|Calymmian|||||||
26072|Nathan Group|22538|4|Described|p710, Fig4, p718|Calymmian||Part of the Favenc package.||||||26-MAR-18
26072|Nathan Group|22600|4|Described|Map legend|Calymmian|Calymmian|||||||
26072|Nathan Group|22644|5|Briefly described|3,5|||Geol. province: McArthur Basin.||||||20-JUL-06
26072|Nathan Group|22662|5|Briefly described|22,23 fig 2|Proterozoic|Proterozoic|Geo.l province: McArthur Basin||||||20-JUL-06
26072|Nathan Group|22664|6|Mentioned|34|Paleoproterozoic|Paleoproterozoic|Geol province McArthur Basin||||||07-NOV-08
26072|Nathan Group|22716|6|Mentioned|p236|||May be equivalent to the Birrindudu Group of the Birrindudu Basin.||||||
26072|Nathan Group|22808|6|Mentioned|7 fig 4|Mesoproterozoic|Mesoproterozoic|||||||
26072|Nathan Group|22853|5|Briefly described|23|Proterozoic|Proterozoic|Overlying unit: Roper Group, underlying unit: McArthur Group.||||||20-JUL-06
26072|Nathan Group|23216|6|Mentioned|p30||Statherian|Age: < 1640 Ma.||||||
26072|Nathan Group|23362|6|Mentioned|339 Fig.2|||||||||
26072|Nathan Group|23374|5|Briefly described|Fig3p5,34,35,6,18,29||Mesoproterozoic|Correlative of Mount Rigg Group. In the McArthur Basin.||||||20-NOV-06
26072|Nathan Group|23387|6|Mentioned|p18 fig.19|||||||||
26072|Nathan Group|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.||||||07-NOV-08
26072|Nathan Group|23395|6|Mentioned|p383|||||||||
26072|Nathan Group|23396|5|Briefly described|p 407 fig.2|||||||||
26072|Nathan Group|23398|5|Briefly described|p443|||||||||
26072|Nathan Group|23405|5|Briefly described|p594|||||||||
26072|Nathan Group|23407|5|Briefly described|p626|||||||||
26072|Nathan Group|23409|5|Briefly described|p536|||In the Isa Superbasin.||||||20-NOV-06
26072|Nathan Group|23733|5|Briefly described|p32 Fig. 19|||Geological Province: MacArthur Basin.||||||
26072|Nathan Group|23776|5|Briefly described|p706|Calymmian|Statherian|Age 1615-1575 Ma.||||||20-JUL-06
26072|Nathan Group|23809|5|Briefly described|protero|Proterozoic|Proterozoic|Geological Province: McArthur Basin.  Correlates with Bullita and Wattie Groups, and Lower Wade Creek Formation of the Victoria Basin.||||||22-NOV-04
26072|Nathan Group|23867|5|Briefly described|p14|Mesoproterozoic|Paleoproterozoic|Geological  Province: McArthur Basin.||||||07-NOV-08
26072|Nathan Group|23902|6|Mentioned|p1568 Fig.1|||Geological Province: McArthur Basin||||||
26072|Nathan Group|23910|4|Described|p290|||Geological Province: McArthur Basin.||||||
26072|Nathan Group|23937|4|Described|p17, p24 Tb. 2|Calymmian|Statherian|Overlain by Phelp Sandstone; unconformably overlies the Vizard Group.  Age: 1614-1589Ma.  Type section in BAUHINIA DOWNS.  Geological Province: McArthur Basin.||||||18-APR-05
26072|Nathan Group|23963|6|Mentioned|p1238|||Geological Province: McArthur Basin.||||||10-MAR-05
26072|Nathan Group|24047|5|Briefly described|p12 Fig. 10, p11|Mesoproterozoic|Mesoproterozoic|Age: 1600-1570?Ma.  Overlies the McArthur Group.  Geological Province: McArthur Basin.||||||
26072|Nathan Group|24048|4|Described|p64|Calymmian|Calymmian|Geological Province: McArthur Basin.||||||
26072|Nathan Group|24049|5|Briefly described|Map Legend|Calymmian|Calymmian|Includes Balbirini Dolomite. Geol. Prov: McArthur Basin.||||||13-OCT-05
26072|Nathan Group|24050|5|Briefly described|p7|Mesoproterozoic|Paleoproterozoic|Age: 1589+/-Ma, 1613+/-4Ma.||||||07-NOV-08
26072|Nathan Group|24122|6|Mentioned|p1|||Geological Province: McArthur Basin.||||||
26072|Nathan Group|24297|5|Briefly described|p1|Proterozoic|Proterozoic|Possibly correlated with Wattie and Bullita Groups. Grological Province: McArthur Basin.||||||
26072|Nathan Group|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.||||||07-NOV-08
26072|Nathan Group|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26072|Nathan Group|40105|6|Mentioned|p310|||||||||
26072|Nathan Group|40109|5|Briefly described|p302|||||||||
26072|Nathan Group|40259|6|Mentioned|Table 1|||||||||
26072|Nathan Group|40691|3|Fully described|p11|||||||||
26072|Nathan Group|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26072|Nathan Group|41019|5|Briefly described|p243|||||||||
26072|Nathan Group|41268|4|Described|p284|||||||||
26072|Nathan Group|41277|5|Briefly described|p80|||||||||
26072|Nathan Group|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
26072|Nathan Group|41721|5|Briefly described|p26, p27|||Includes the Balbirini Dolomite. Geological Province: McArthur Basin.||||||01-AUG-07
26072|Nathan Group|42385|4|Described|p23|||See also Table 4 p16.||||||20-NOV-06
26072|Nathan Group|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
26072|Nathan Group|42395|6|Mentioned|Fig.26 P86|||||||||
26072|Nathan Group|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.|||Includes: Dungaminnie Formation, Balbirini Dolomite and Smythe Sandstone.|Shown in legend as adjacent to Karns Dolomite. Underlies Lower Roper Group (Roper Group) units; overlies Batten Subgroup (McArthur Group) units.||07-NOV-11
26072|Nathan Group|42639|4|Described|p35, Table 6|||||||||
26072|Nathan Group|42700|5|Briefly described|map legend|Mesozoic|Early Cretaceous|||||||
26072|Nathan Group|42739|5|Briefly described|map legend|Calymmian|Calymmian|Cyclic dolostone, dolarenite, sandstone, mudstone, evaporite casts, basic to intermediate volcanics, feldspathic sandstone, tuffite.||||||19-OCT-05
26072|Nathan Group|42812|3|Fully described|p42, Table 4|||||||||
26072|Nathan Group|42846|5|Briefly described|p503, Fig.1 p502|||Geological Province: McArthur Basin.||||||09-MAY-05
26072|Nathan Group|42935|6|Mentioned|p527|||||||||
26072|Nathan Group|43010|6|Mentioned|Table 14.|||||||||
26072|Nathan Group|43036|5|Briefly described|p55|||||||||
26072|Nathan Group|43292|5|Briefly described|Map Legend||Mesoproterozoic|||||||
26072|Nathan Group|43486|5|Briefly described|21|||||||||
26072|Nathan Group|43595|4|Described|p438||Mesoproterozoic|||||||
26072|Nathan Group|43788|6|Mentioned|p13||Proterozoic|||||||
26072|Nathan Group|44112|4|Described|p63,65|||Part of Supersequence 4||||||
26072|Nathan Group|45162|2|Defined|p136|Proterozoic|Proterozoic|Mention p45.||||||20-NOV-06
26072|Nathan Group|50225|5|Briefly described|p406 Fig. 10, p407|Mesoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.||||||07-FEB-11
26072|Nathan Group|60483|4|Described|p7 Fig. 5, p9, p32|||Incl: Kookaburra Ck and Dungaminnie Fm, Mt Birch and Smythe Ssts, and Balbirini Dolomite. Unconform.over McArthur Gp.and under Roper Gp. Thickness: 700m. Geol.Prov: McArthur Basin. Correlates with Karns Dolomite.||||||05-OCT-07
26072|Nathan Group|60558|5|Briefly described|p7, p8 Fig. 6|Proterozoic|Proterozoic|Includes four units. Dominated by shallow water to locally emergent, often evaporitic carbonates with minor associated fine-grained shallow water clastics.||||||
26072|Nathan Group|60573|5|Briefly described|Map legend|Calymmian|Statherian|Includes Walmudga, Yalwarra, Kookaburra Creek Formations and Mount Birch Sandstone.  Overlain by Phelp Sandstone. Does not outcrop in the ROPER RIVER mapsheet area.||||||20-JUL-06
26072|Nathan Group|60574|5|Briefly described|Map Legend|||Geological Province: McArthur Basin.||||||
26072|Nathan Group|60682|6|Mentioned|p6|||Geological Province: Macarthur Basin.||||||
26072|Nathan Group|60685|5|Briefly described|p1|||Geological Province: McArthur Basin.||||||
26072|Nathan Group|61390|5|Briefly described|Map Legend|Calymmian|Statherian|||||||
26072|Nathan Group|61403|5|Briefly described|Map Legend|Calymmian|Calymmian|Includes Balbirini Dolomite. Geol. Prov: McArthur Basin.||||||
26072|Nathan Group|63112|6|Mentioned|p1190|||Southern McArthur Basin.||||||
26072|Nathan Group|63866|5|Briefly described|p113-p114, p116-p117, p123|||Walker Fault Zone, northern and central Caledon Shelf and Urapunga Fault Zone.|<1710 Ma (unit relationships)|||Unconformably overlain by the Roper Group. Unconformably overlies the West Branch Volcanics, Mount Bonner Sandstone and the Jalma Formation. Equivalent to the Mount Rigg Group.||
26072|Nathan Group|64724|5|Briefly described|p45 Fig.5, p46, 47|Calymmian|Statherian|McArthur Basin unit deposited as part of sedimentation in the Isa Superbasin (1660-1590 Ma)||||||
26072|Nathan Group|64784|6|Mentioned|p3 Fig.3 |||||||||
26072|Nathan Group|64815|5|Briefly described|p3, p11, p13, p15 Fig.9 |Calymmian|Statherian|See also p16-18 Figs.10-12, p17, p19. Rawlings (1999) assigned the lower part of the Nathan Group to the McArthur Group.|1613 +/- 4 Ma and 1609 +/- 3 Ma.||Includes Balbirini Dolostone, Smythe Sandstone and Dungaminnie Formation.|Generally unconformably overlies the McArthur Group.|Dolostone; basal polymict conglomerate and pebbly lithic (chert) sandstone; beds of fine sandstone and siltstone.|
26072|Nathan Group|64816|6|Mentioned|p2 Fig.1, p4  |||||||||
26072|Nathan Group|64817|6|Mentioned|p352 Fig.3, p353 Fig.4 ||||||Includes Balbirini Dolomite, Kookaburra Creek Formation, Mount Birch Sandstone, Dungaminnie Formation, Smythe Sandstone.|||
26072|Nathan Group|64975|6|Mentioned|p162 Fig.6.|Mesoproterozoic|Mesoproterozoic|||||||
26072|Nathan Group|65228|4|Described|p7, p9, pp38-39, Fig.02.|Statherian|Statherian|McArthur Basin. Mixed carbonates and clastics. 1,200 m thick. Contains discontinuities.|1614-1610 Ma.||Includes Smythe Sandstone, Balbirini Dolomite and Dungaminnie Formation.|Unconformably overlies McArthur Group. Is overlain unconformably by Roper Group.||
26072|Nathan Group|65232|6|Mentioned|p5 Fig. 4|||Presented as Nathan and Mount Rigg groups on figure. Geol. Prov: Pine Creek Orogen.||||||09-FEB-10
26072|Nathan Group|65236|6|Mentioned|p4 Fig. 4|||Geological province: Beetaloo Sub-basin.||||||
26072|Nathan Group|65337|6|Mentioned|p7.||||c.1590 (Jackson et al. 2000b).|||||
26072|Nathan Group|65340|5|Briefly described|p57, p59, p10-11.|||Batten Trough. Possible partial correlation with Karns Dolomite, although characteristic pink tuffite beds of this unit have not been observed in the Karns Dolomite.|1589 +/- 3 Ma (Jackson et al. 2000b) medial Group.|||||26-MAR-18
26072|Nathan Group|65342|5|Briefly described|p8.|||McArthur Basin. Max. thickness at least 437 m.||||Is overlain by Mantungula Formation.|Dolostone, chert, dolomitic sandstone, siltstone.|
26072|Nathan Group|66843|4|Described|p23-26, p34, p37-39|||Southern McArthur Basin. Composite stratigraphic column; gamma-ray curve. Lithofacies described in great detail, organised in 9 cycles. Evolution of the Group is revised in this study.|||Includes Balbirini Dolomite, Dungaminnie Formation.|Unconformably overlies McArthur Group. Is overlain unconformably by Roper Group.|A succession of stromatolitic carbonates with minor sandstone and shale.|12-SEP-19
26072|Nathan Group|67144|5|Briefly described|Map legend.|Calymmian|Calymmian|McArthur Basin.|||Includes Balbirini Dolostone.|Overlies McArthur Group. Is overlain by Roper Group.||13-APR-12
26072|Nathan Group|67269|6|Mentioned|p20-21 Fig.19|||McArthur Basin.|||Dungaminnie Formation.|||
26072|Nathan Group|67323|5|Briefly described|Eastern Australia Time-Space Plot; p9|||NT (Jackson & Southgate 2000). Supersequences extend on to Lawn Hill Platform.|||Includes Yalwarra Volcanics and unconformity-bounded Lawn, Wide and Doom Supersequences.|||
26072|Nathan Group|67352|4|Described|v, p11,  p13 Tb.2, p51|Calymmian|Statherian|McArthur Basin. 1.6 km thick. Deposition terminated by Isan Orogeny.|1615-1575 Ma||Balbirini Dolostone, Smythe Sandstone.|Overlies McArthur Group paraconformably. Overlain by Roper Group (unconformably).|Dominated by stromatolitic and evaporitic dolostone; basal conglomerate and pebbly lithic sandstone.|
26072|Nathan Group|67564|5|Briefly described|p51.|Mesoproterozoic|Paleoproterozoic|Southern McArthur Basin. Correlative of Mount Rigg Group in Pine Creek Orogen.|1613 - 1590 Ma.|||||
26072|Nathan Group|68280|6|Mentioned|p26 fig 24|||McArthur Basin.|||Includes Dungaminnie Formation|||
26072|Nathan Group|69018|5|Briefly described|p450 Fig.1a, b|Calymmian|Statherian|Of McArthur Basin.|||Includes Balbirini Dolomite, Dungaminnie Formation.|||
26072|Nathan Group|69417|6|Mentioned|p2:5|Calymmian|Statherian|McArthur Basin.||||||12-JUL-16
26072|Nathan Group|69429|5|Briefly described|p14:3 Fig.14.4, 14:4|Mesoproterozoic|Mesoproterozoic|McArthur Basin. Hosts quartz hematite (ironstone) lenses (the Murphys Fe prospect).|||Mount Birch Sandstone.|||12-JUL-16
26072|Nathan Group|69430|4|Described|p15:2-4, 9, 16, 19, 21-25, 27, 29-30, 61|||Jackson et al. (1987), for units overlying a regional unconformity within the upper part of the revised (Plumb and Brown, 1973) McArthur Group, but underlying the Roper Group. McArthur Basin. Fair to good conventional hydrocarbon reservoirs occur.|||Balbirini, Karns Dolostones; Mount Birch, Smythe Sandstones; Knuckey, Walmudga, Dungaminnie Formations; Yalwarra Volcanics.|Unconformably overlies Amos Formation (Batten Subgroup, McArthur Group), Bath Range Formation (Balma Group), Vizard and Tawallah Groups. Is overlain unconformably by Roper Group.|Includes a relatively thin and lenticular basal siliciclastic and often conglomeratic unit, overlain by thicker carbonate and siliciclastic rocks.|12-JUL-16
26072|Nathan Group|69591|6|Mentioned|p47|||Northern Territory. Includes the Term, Lawn, Wide and Doom Supersequences.||||||
26072|Nathan Group|69673|4|Described|vii, p3 fig 2, p15, p32, p41|Paleoproterozoic|Paleoproterozoic|Fair to good conventional reservoir properties.|||Includes Balbarini Dolostone, Walmudga Formation, Yalwarra Volcanics, Knuckey Formation, Mount Birch Sandstone, Smythe Sandstone, Dungaminnie Formation, Karns Dolostone|Unconformably overlies McArthur Group|Basal fluvial chert-clast sandstone overlain by stromatolitic and ooidal dolostone; minor siliciclastic sandstone.|
26072|Nathan Group|70822|5|Briefly described|p102 fig 1 (A), p103|Mesoproterozoic|Mesoproterozoic||1589 +/- 3 Ma.|||Overlies McArthur Group. Overlain unconformably by Phelp Sandstone (Roper Group).||
26072|Nathan Group|70897|5|Briefly described|p42-45|||Correlated with upper part of South Nicholson Group. Uppermost units deposited c.1590 Ma.|||Dungaminnie Formation, Balbirini Dolomite.|Is overlain unconformably by Roper Group.|Tightly folded and faulted carbonate-rich succession.|
26072|Nathan Group|70968|5|Briefly described|p2 Fig.3,p6-8,p10,p13,p123,p132,p138-139|Calymmian|Statherian|On detrital zircon and lithological grounds, doubt is cast on the general acceptance of equivalence of this unit with Bullita and Wattie Groups. SHRIMP U-Pb zircon age of a tuff in the upper part of the Group.|1589 +/- 3 Ma (Page et al., 2000).||Walmudga Formation.|Is overlain unconformably by Phelp or Limmen Sandstones (Roper Group).||
26072|Nathan Group|71059|5|Briefly described|p1-3, p7|Mesoproterozoic|Mesoproterozoic|McArthur Basin.||||Is overlain unconformably by Phelp Sandstone (Roper Group). Equivalent to Wattie and Bullita Groups (Birrindudu Basin).||
26072|Nathan Group|71374|5|Briefly described|iii, p1 tbl 1, p2, p6, p18, p30, p33|Mesoproterozoic|Palaeoproterozoic|McArthur Basin.|||Includes the Smythe Sandstone, Balbirini Dolostone and Karns Dolostone.|Overlies the McArthur Group, Habgood Group and Balma Group. Equivalent to the Bullita and Wattie Groups.||
26072|Nathan Group|71488|6|Mentioned|p141 fig 1b|Mesoproterozoic|Mesoproterozoic|||||Unconformably overlain by the Roper Group.||
26072|Nathan Group|71606|5|Briefly described|p135,137-138|Calymmian|Calymmian|Walker Trough, Caledon Shelf, Bauhinia Shelf and Batten Trough; McArthur Basin. Evaporite-carbonate sequence deposited in a broad sag basin across most of the region with no evidence of tectonic control from previous rifts. Correlable to Mount Rigg Group and Karn Dolomite.||||Overlain unconformably by Roper Group. Underlain unconformably by Balma Group, Vizard Formation, Spencer Creek Group, Tawallah group and McArthur Group.||
26072|Nathan Group|71632|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|McArthur Basin.|||Includes Yalwarra Volcanics.||Cyclic coarse-grained evaporitic-stromatolitic-ooidal dolostone, sandstone, siltstone; minor conglomerate; synsedimentary basaltic sills, sandstone, mudstone (Yalwarra Volcanics).|05-MAR-20
26072|Nathan Group|71779|5|Briefly described|p5|Mesoproterozoic|Palaeoproterozoic|McArthur Basin.||||Disconformably or unconformably overlain by the Roper Group.||
26072|Nathan Group|71893|4|Described|p9, p13|Calymmian|Calymmian|McArthur Basin. SHRIMP age is derived from a tuff in this unit.|1589 +/-3 (SHRIMP, Page et al, 2000)||Includes the Walmudga Formation.|Unconformably overlain by the Phelp Sandstone and the Limmen Sandstone (Collara Subgroup) .||
26072|Nathan Group|72248|5|Briefly described|p146,148|||Of McArthur Basin.|||||Dolostone with lesser sandstone and fine-grained clastics.|
26072|Nathan Group|72373|5|Briefly described|iii,p1-2,37-28,33,36,39|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.|||Includes Smythe Sandstone, Balbirini Dolostone, Knuckey Formation and Mount Birch Sandstone.|Underlain by Balma Group.||
26072|Nathan Group|72377|5|Briefly described|p13|Mesoproterozoic|Paleoproterozoic|Of McArthur Basin.|||Includes Balbirini Dolostone.|||10-OCT-19
26072|Nathan Group|72381|5|Briefly described|p772|||Of [or under?] Beetaloo Sub-basin, McArthur Basin.||||Overlain unconformably by Cororan Formation.||03-OCT-19
26072|Nathan Group|72523|5|Briefly described|piii, p1, p1 Fig.1, p2 Fig.2, p8, p12.|Early Mesoproterozoic|Early Mesoproterozoic|Described as part of the Favenc package (Rawlings 1999).|||Includes Smythe Sandstone, Balbirini Dolostone, Dungaminnie Formation and Knuckey Formation.|Unconformably overlies Amos Formation, McArthur and Tawallah groups. Unconformably overlain by Roper Group.||
26072|Nathan Group|72526|5|Briefly described|p8 Fig.1.3.|Calymmian|Statherian|Shown as being located in the Urapunga Fault Zone in the Southern McArthur Basin. Part of the Favenc package (Lithostratigraphic package).|||Walmudga Formation, Yalwarra Volcanics, Knuckey Formation, Mount Birch Sandstone, Balbirini Dolostone, Smythe Sandstone, Dungaminnie Formationh and Karns Dolostone.|Shown as overlying Vizard Group, McArthur Group and shown as unconformably underlying Roper Group.||
26072|Nathan Group|72527|6|Mentioned|p10.|Paleoproterozoic|Paleoproterozoic|Dating of this group has assisted in constraining maximum depositional ages for the South Nicholson Group.|||Includes Balbirini Dolostone.||Includes tuffs.|
26072|Nathan Group|72718|6|Mentioned|piii, p5-9|Mesoproterozoic|Mesoproterozoic|Beetaloo Sub-basin, McArthur Basin. Isa Superbasin, Favenc package. A tuff in the upper portion of the group yielded a SHRIMP U-Pb zircon age of 1589 +/- 3 Ma.|||Wakmudga Formation, Yalwarra Volcanics, Knuckey Formation, Mount Birch Sandstone.|Unconformably underlain[?] by Nagi Formation (Vizard Group). Unconformably overlain by Phelp Sandstone and[?] Mantungula Formation (both of Collara Subgroup, Roper Group).||
26072|Nathan Group|72912|5|Briefly described|p5 Fig.3, p18.|Calymmian|Statherian|This group extends across all of the  Southern McArthur Basin.|||Walmudga Formation, Yalwarra Volcanics, Knuckey Formation, Mount Birch Sandstone, Dungaminnie Formation, Balbirini Dolostone, Smythe Sandstone and Karns Dolostone.|Unconformably underlies Roper Group and unconformably overlies Vizard and McArthur Groups.||
26072|Nathan Group|73042|6|Mentioned|p4|Mesoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.|||Walmudga Formation, Yalwarra Volcanics, Knuckey Formation, Mount Birch Sandstone, Dungaminnie Formation, Upper Balbirini Dolostone, Smythe Sandstone, Karns Dolostone.|Unconformably underlain(?) by Vizard Group and McArthur Group. Unconfrmably overlain by Roper Group.||
26072|Nathan Group|73242|6|Mentioned|p39|||||||Overlain by[?] Phelp Sandstone, Collara Subgroup, Roper Group.||
26072|Nathan Group|73280|6|Mentioned|p1, p4-5, App.1A, App.1B, App.1C|||McArthur Basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report].||||||
26072|Nathan Group|73412|4|Described|p2, 4, 6, 8, 10-11, 13, 15-19|||Southern McArthur Basin. Dry bulk density tabulated.|c.1610-1580 Ma.||Smythe Sandstone, upper Balbirini Dolostone, Dungaminnie Formation, Karns Dolostone.|Unconformably overlies McArthur and (locally) Tawallah Groups. Is overlain unconformably by Roper Group.|Siliciclastic and carbonate rocks with minor intercalated mafic volcanics.|
77536|Navajo Sandstone|66880|6|Mentioned|pp10-11, p28.|Archean|Archean|Fluvial deposits underlying the Kurrawang Sequence.|Detrital zircons 2657 +/- 4 Ma.|||||
77536|Navajo Sandstone|68289|5|Briefly described|p15|||Krapez et al (2008) interpreted it as a fluvial deposit based on sedimentary features. However Squire et al (2010) argue for a volcanic source of deposition on the basis of textural immaturity and volcanic quartz grains.|2670-2660 Ma|||Equivalent to the Merougil Formation.|Coarse-grained, quartz-rich, typically well-sorted sandstone with minor conglomerate containing felsic clasts.|
77536|Navajo Sandstone|69631|5|Briefly described|p18|Neoarchean|Neoarchean|Possibly a large-volume, quartz-rich pyroclastic flow deposit.|c.2670-2660 Ma (Krapez et al., 2000).|||Unconformably overlies Black Flag Group. Is overlain unconformably by Kurrawang Formation. Correlated with Merougil Formation.|Coarse-grained, quartz-rich, typically well-sorted sandstone with minor conglomerate containing felsic clasts.|
77536|Navajo Sandstone|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2657 +/- 4 Ma (isotopic) - 2640 Ma (inferred).||||Quartz-rich sandstone with subordinate cobble-pebble conglomerate; tabular to trough cross-bedding; local clast-supported conglomerate; metamorphosed.|
77536|Navajo Sandstone|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma); Yilgarn Craton events (4000 - 2600 Ma).|2657+\-4 Ma; 2640 Ma||||Quartz-rich sandstone with subordinate cobble--pebble conglomerate; tabular to trough cross-bedding; local clast-supported conglomerate; metamorphosed|
77536|Navajo Sandstone|72049|5|Briefly described|p256-p257, p259, p268|||Geochronology analyses, results, and interpretation are discussed in detail.|2657 +/- 4 Ma (SHRIMP U-Pb)|Early Merougil Group||||
77536|Navajo Sandstone|72095|6|Mentioned|p6, p8|Neoarchean|Neoarchean|Eastern Goldfields, Yilgarn Craton.|<2657 Ma|||||
77536|Navajo Sandstone|73391|4|Described|p53, 69, 74, 78, 86-88, 90-96, 99-101|||See also p175-176, 179, 219, 236, 242, 245, 304, 390, 403, 411, Appendices. Ora Banda Domain, Kalgoorlie Terrane. Exposed at the Binduli mining centre; type section is at Binduli. Is shown as a unit within Kurrawang Formation but is only once given the rank of member [sic]. Stratigraphic column, photographs.|2655 +/- 5 Ma (Fletcher et al., 2001).|Basal Kurrawang Formation.||Unconformably overlies Upper Black Flag Formation. Is overlain unconformably by Kurrawang Conglomerate.|Strongly siliciclastic/polymictic, trough cross-bedded quartz sandstone with pebbly quartz-sandstone and polymictic conglomerate. ~250m thick. Fluvial deposits.|
78534|Navigator Monzogranite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||3010 - 2600 Ma (inferred).||||Biotite monzogranite.|
78534|Navigator Monzogranite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2680-2600 Ma (inferred)||||Biotite monzogranite|
81033|Neale Supersuite|70802|5|Briefly described|250k_pre_mesozoic_interpgeop_lut.csv|||Geological province: Albany-Fraser Orogen, West Australian Craton. |||Includes Hercules Gneiss.|||
81033|Neale Supersuite|72034|6|Mentioned|500k_interpgeop16_lut|Paleoproterozoic|Neoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Hercules Gneiss.|||
77414|Nebo-Babel intrusion|65693|5|Briefly described|pp12-14.|||Gabbroic rocks with similar geochemistry occur to the north of the Cavenagh Range and east at the Saturn pluton. Shows close compositional similarities with Alcurra Dolerite and Kullal Dyke Suite.|||||Gabbronorites, hosting orthomagmatic Cu-Ni-PGE mineralization.|
26073|Neerigen Formation|30939|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26073|Neerigen Formation|33044|6|Mentioned|Map 3.|||Pt. of Cardup Gp.||||||
26073|Neerigen Formation|36293|2|Defined|p72|Neoproterozoic|Neoproterozoic|Type section; road cutting 300 m N of the "Olde Narrogin Inne" at Armadale. Thickenss: 23.6m at type section. Formation is cut by dolerite dykes.||Of Cardup Group.||Conformably overlies Whitby Sandstone or unconformably overlies Archean rocks. Is conformably overlain by Armadale Shale.|Interbedded fine to medium grained, micaceous, poorly sorted, thin to medium bedded sandstone interbedded with fissile, in part sandy and silty, shale.|19-DEC-13
26073|Neerigen Formation|36872|3|Fully described|p78|||||||||
26073|Neerigen Formation|37460|6|Mentioned|p178|||||||||
27520|Negri Subgroup|14019|4|Described|p21|Middle Cambrian|Middle Cambrian|Of the Goose Hole Group.  Includes Headleys Limestone, Nelson Shale, Linnekar Limestone and Panton Formation.  Underlies the Elder Subgroup (Goose Hole Group).  Max. thickness: 530m.  Geological Province: Ord Basin.||||||25-JUL-06
27520|Negri Subgroup|22547|5|Briefly described|p30|||Of the Goose Hole Group. Overlain by Elder Subgroup.||||||14-NOV-06
27520|Negri Subgroup|23621|5|Briefly described|p36|Late Cambrian|Middle Cambrian|See also page 9 Table 1. Of Goose Hole Group. Geological Province: Ord Basin.||||||
27520|Negri Subgroup|40993|6|Mentioned|Fig.1|||||||||
27520|Negri Subgroup|41840|4|Described|p41|||Formerly Negri Group, "Negri Series"||||||
27520|Negri Subgroup|41864|4|Described|p18|||Formerly Negri Group, "Negri series"||||||
27520|Negri Subgroup|41865|6|Mentioned|Map legend|Middle Cambrian|Early Cambrian|||||||
27520|Negri Subgroup|41866|5|Briefly described|Map legend|Middle Cambrian||||||||
27520|Negri Subgroup|43299|5|Briefly described|Map Legend||Cambrian|of Goose Hole Group.||||||
27520|Negri Subgroup|43819|6|Mentioned|p31||Early Cambrian|||||||
27520|Negri Subgroup|43853|5|Briefly described|Map Legend||Ordian|||||||
27520|Negri Subgroup|43855|5|Briefly described|Map Legend||Ordian|||||||
27520|Negri Subgroup|44230|5|Briefly described|Map Legend||Middle Cambrian|||||||
27520|Negri Subgroup|44868|5|Briefly described|Map Legend|Boomerangian|Ordian|||||||
27520|Negri Subgroup|60419|4|Described|p1, p3 Fig.2|Middle Cambrian|Middle Cambrian|Of Goose Hole Group. Conformably overlain by Elder Subgroup. Peritidal, with marine incursions. Max. thickness: 530 m. Geological Province: Ord Basin.||||||
27520|Negri Subgroup|60519|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Goose Hole Group. Includes: Headleys Limestone, Nelson Shale, Linnekar Limestone, Panton Formation. Geological Province: Ord Basin.||||||03-NOV-04
27520|Negri Subgroup|60589|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Goose Hole Group.  Geological Province: Ord Basin.||||||
27520|Negri Subgroup|67860|5|Briefly described|p417, p419 Tb. 4-18, p421 fig 4-86|Middle Cambrian|Middle Cambrian|160-530 m thick.||Goose Hole Group|Includes Headleys and Linnekar Limestones; Nelson Shale; Panton Formation.|Conformably overlies Antrim Plateau Volcanics. Is overlain conformably by Elder Subgroup. Equivalent to Tarrara Formation (Bonaparte Basin).|Mainly siltstone and mudstone; minor limestone, sandstone and gypsum.|
27520|Negri Subgroup|69099|4|Described|GEOL_LUT_CSV files + geochron files|Cambrian||Ord Basin||Goose Hole Group|Includes Panton Formation, Linnekar Limestone, Nelson Shale, Headleys Limestone||Siltstone, shale, limestone.|03-AUG-15
27520|Negri Subgroup|69165|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian|See also 100k_xsecgeop_lut.csv. ||Goose Hole Group|Includes Panton Formation, Linnekar Limestone, Nelson Shale, Headleys Limestone||Undivided, siltstone, shale and limestone.|
27520|Negri Subgroup|69437|5|Briefly described|p22:11|Cambrian|Cambrian|Ord Basin, Centralian B Superbasin. Sequence 1. Dominantly peritidal and lesser shallow-marine deposits.|||Headleys, Linnekar Limestones; Nelson Shale; Panton Formation.|Equivalent to Tarrara, Gum Ridge, Border Waterhole, Chandler Formations; Thorntonia, Tindall, Top Springs Limestones; Walbiri, Giles Creek Dolostones.|Fine-grained siliciclastic rocks and limestone.|12-JUL-16
27520|Negri Subgroup|69448|4|Described|p33:1-6, 8|Late Cambrian|Middle Cambrian|Ord Basin. Up to 530m thick. Fossils allow correlation with Tindall Limestone (Daly Basin), Montejinni Limestone and Hooker Creek Formation (Wiso Basin), Top Springs Limestone/Gum Ridge Formation/Thorntonia Limestone/Border Waterhole Formation (Georgina Basin).||Goose Hole Group.|Headleys, Linnekar Limestones; Nelson Shale; Panton Formation.|Disconformably overlies Antrim Plateau Volcanics. Is overlain conformably and gradationally by Elder Subgroup. Is broadly correlated with Tarrara Formation (Bonaparte Basin).|Dominantly maroon gypsiferous siltstone and mudstone, punctuated by three brief marine carbonate incursions.|12-JUL-16
27520|Negri Subgroup|69634|5|Briefly described|100k_interpgeop_lut.csv|||||Unit of Goose Hole Group.|Includes Headleys Limestone, Linnekar Limestone, Nelson Shale, Panton Formation.|||
27520|Negri Subgroup|69673|6|Mentioned|p192, p193|Cambrian|Cambrian |||Goose Hole Group|Includes Headleys Limestone, Nelson Shale, Linnekar Limestone, Panton Formation||Gypsiferous silstone and mudstone.|
27520|Negri Subgroup|70154|6|Mentioned|100k_interpgeop_lut.csv|Ordovician|Cambrian||485-509 Ma|Goose Hole Group|Includes Panton Formation, Linnekar Limestone, Nelson Shale, Headleys Limestone|||
27520|Negri Subgroup|71146|5|Briefly described|p6|Cambrian|Cambrian|Ord Basin.||Goose Hole Group||Overlies the Antrim Plateau Volcanics. Overlain by the Elder Subgroup.|Mudstone and carbonate.|
27520|Negri Subgroup|71267|4|Described|GEOL_LUT_CSV files|||Geological province: Halls Creek Orogen. Of Ord Basin. See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.||Unit of Goose Hole Group.|Includes Headleys Limestone, Linnekar Limestone, Nelson Shale, Panton Formation.||Micritic and stromatolitic limestone and chert; siltstone, calcareous mudstone; minor feldspathic sandstone|
27520|Negri Subgroup|71800|4|Described|p25-p26|Middle Cambrian|Middle Cambrian|Ord Basin. Deposited in intertidal to shallow subtidal environments.||Goose Hole Group|Includes the Headleys Limestone, Nelson Shale, Linnekar Limestone and the Panton Formation.|Overlain by the Elder Subgroup.||
34469|Neil Creek Monzogranite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.||||||07-NOV-08
34469|Neil Creek Monzogranite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1850Ma. Geological province: Kimberley Province (East).||||||07-FEB-11
34469|Neil Creek Monzogranite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
34469|Neil Creek Monzogranite|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite.||||||07-NOV-08
34469|Neil Creek Monzogranite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Paperbark Supersuite.|||Fine- to medium-grained, weakly porphyritic monzogranite|
75828|Nelson Rocks Formation|13255|6|Mentioned|p369|Late Cretaceous|Early Cretaceous|Roebuck Basin.||||Overlies Mermaid Formation. Is overlain by Toolonga Calcilutite.||
75828|Nelson Rocks Formation|66193|5|Briefly described|p569 Fig.2|Late Cretaceous|Early Cretaceous|in offshore Canning Basin, overlies the Mermaid Formation, underlies the Toolonga Calcilutite||||||
75828|Nelson Rocks Formation|69297|6|Mentioned|p337, p352|Turonian|Aptian|Canning and Roebuck Basins. ||||Overlies the Mermaid Formation. Unconformably overlain by the Toolonga Calcilutite.||
75828|Nelson Rocks Formation|69689|6|Mentioned|p16|Cretaceous|Cretaceous|Roebuck Basin.||||Overlies Mermaid Formation.||
75828|Nelson Rocks Formation|70065|5|Briefly described|Rowley: Fig.2. Regional: Fig.4|Turonian|Aptian|Roebuck Basin and offshore Canning Basin.||||Overlies Mermaid Formation. Is overlain by Toolonga Calcilutite.||
80965|Neoproterozoic-Cambrian sedimentary rocks, Amadeus Basin 80965|72034|5|Briefly described|500k_interpgeop16_lut|Cambrian|Neoproterozoic|Amadeus Basin (Phase 1). Informal, group rank.|||||Sandstone, minor siltstone and conglomerate.|
73468|Nerrely Leucogranite|63372|4|Described|Map Legend|Archean|Archean|Geological Province: Hamersley Basin. Age: 2765Ma. Biotite (-tourmaline)-bearing leucogranite; unfoliated.||||||23-DEC-09
73468|Nerrely Leucogranite|64174|5|Briefly described|Map legend|Archean|Archean|Leucogranite, unfoliated. Geological province: Hamersley Basin.||||||07-NOV-08
73468|Nerrely Leucogranite|64580|4|Described|map legend||Neoarchean|Biotite(-tourmaline)-bearing leucogranite; unfoliated.||||||15-DEC-08
73468|Nerrely Leucogranite|69185|5|Briefly described|500k_geologyp08_lut.csv||Neoarchean||||||Biotite(-tourmaline)-bearing leucogranite; unfoliated|
73468|Nerrely Leucogranite|69299|5|Briefly described|p8 Fig.5, p15, p21|||Mallina Basin. Intrusion on MOUNT WOHLER. Mentioned as previously incorrectly named the Opaline Well Granite. Age from Nelson (1997); Smithies (1998b); Smithies and Hickman (2003).|c. 2765 Ma|||||
73468|Nerrely Leucogranite|69300|5|Briefly described|map legend|Archean|Archean|Hamersley Basin. Isotopic age: shown on legend as c.2765 Ma|2765 +/- 5 Ma (isotopic age, Nelson 1997)||||biotite(-tourmaline)-bearing leucogranite; unfoliated|
73468|Nerrely Leucogranite|70775|6|Mentioned|p41||||c. 2765 Ma|||||
73468|Nerrely Leucogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite, tonalite, monzogranite, granodiorite|
73468|Nerrely Leucogranite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Fortescue Basin.|2765+/-5 Ma.||||Biotite(-tourmaline)-bearing leucogranite; undeformed.|
29784|Netty Dolerite|43038|6|Mentioned|p26|||||||||
77939|Never Can Tell Basalt|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2720 - 2680 Ma (inferred).|Two Sisters Subgroup|||Fine-grained mafic schist; minor intercalated metasedimentary rock. Basalt; fine grained with local pyroxene-spinifex texture; includes medium-grained layers and lenses; metamorphosed.|
77939|Never Can Tell Basalt|70326|3|Fully described|p334,336,338-9,341-3,346,349-351, p354,|Neoarchean|Neoarchean|Geological province: Agnew region, Ora Banda Domain, Kalgoorlie Terrane, Yilgarn Craton. Subaqueous extrusive high-Fe tholeiitic basalts that are highly fractionated and enriched in incompatible elements. The extrusive pil eis intruded by a late, even more fractionated and enriched, comagmatic sill. Thickness: ~300m. Lithofacies include upper basalt (?150 m), middle intrusion (?100 m) and lower basalt (?50 m). Observed in several drillholes on the Agnew Anticline western limb, and sporadically in outcrop across the study area. Intruded by several sills of the Bounty Igneous Complex. Major and trace element geochemical analysis on Table 4 p342-346. Evidence of crustal contamination e.g. negative Nb and T ianomalies; [La/Sm]PM> 1; Pearce, 2008; van Hunen and Moyen, 2012). Weighted mean 207Pb/206Pb date of 2711+\-4 Ma, interpreted to be depositional age of sampled sediment (air-fall deposit from a distal felsic pyroclastic eruption). See also p353-4,358-65. See also p364.||||Overlain by Agnew Komatiite. Correlable to Missouri, Centenary Bore, and Lindsay basalts.|Massive basalt,minor dolerite underlain by dolerite, gabbro, minor basalt; lower section: massive/pillowed basalt (feldspar phyric). Includes thin mudstone intervals. Submarine sheet flows (upper and lower basalts) and comagmatic intrusion (middle).|29-JUL-19
77939|Never Can Tell Basalt|71212|5|Briefly described|intro p2, intro p3|||Yilgarn Craton. ||||Intruded by the Golden Empress, Wildcat and Mikado Gabbros. Overlies the Bounty Igneous Complex. Overlain by the Agnew Komatiite.|Tholeiitic mafic volcanics|
77939|Never Can Tell Basalt|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2711-2687 Ma (inferred)|Unit of Two Sisters Subgroup.|||Basalt; fine grained with local pyroxene-spinifex texture; includes medium-grained layers and lenses; metamorphosed; Fine-grained mafic schist; minor intercalated metasedimentary rock.|
77939|Never Can Tell Basalt|73151|5|Briefly described|p3, p10, p12-13, p16|Neoarchean|Neoarchean|Yilgarn Craton. Kalgoorlie Terrane, Agnew Greenstone Belt.||Kalgoorlie Group||Overlies Songvang Formation, underlies Agnew Komatiite.|Basalt.|
77939|Never Can Tell Basalt|73596|6|Mentioned|p1152-1153, 1156-1158, 1160, 1162-1163|Neoarchean|Neoarchean|See also p1165, 1167. Agnew-Wiluna Greenstone Belt. Age from an interflow tuff horizon. Deep-water mafic-ultramafic lava fields and feeder intrusions.|2711 +/- 4 Ma.|Basal Two Sisters Subgroup.||Unconformably overlies Songvang Basalt, Cosmos Volcanic Complex. Is overlain by Agnew Komatiite.||
22528|Neville Granodiorite|22754|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of the Paperbark suite.  Age: c.1860Ma.||||||07-NOV-08
22528|Neville Granodiorite|23323|5|Briefly described|p456 Table 1|Orosirian|Orosirian|Age: 1860 +/- 4 Ma.||||||07-FEB-07
22528|Neville Granodiorite|23383|4|Described|p5 Tb.1, p8|Paleoproterozoic|Paleoproterozoic|Of Paperbark Supersuite in the Lamboo Complex.  Age: 1860 +/- 3 Ma (SHRIMP U-Pb Zircon age). Intrudes the Marboo Formation. Geological Province: Hooper Orogen.||||||07-NOV-08
22528|Neville Granodiorite|23601|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|medium- to fine-grained biotite granodiorite and tonalite; minor monzogranite.  In the Lamboo Complex.||||||07-NOV-08
22528|Neville Granodiorite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1850Ma. Geological province: Kimberley Province (East).||||||07-FEB-11
22528|Neville Granodiorite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
22528|Neville Granodiorite|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite. Medium- to fine-grained biotite granodiorite; minor monzogranite; metasedimentary rock inclusions are abundant adjacent to contacts with metasedimentary rock. Age:1865-1850Ma.  In the Hooper / Lamboo Complex (western zone)||||||07-NOV-08
22528|Neville Granodiorite|44694|5|Briefly described|Map Legend||Proterozoic|||||||
22528|Neville Granodiorite|50437|5|Briefly described|p1.5, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite. Age: 1860 +/- 3Ma (Shrimp).||||||07-NOV-08
22528|Neville Granodiorite|63866|5|Briefly described|p132|||Western Zone, Halls Creek Orogen.|c. 1860 Ma|Paperbark Supersuite||||
22528|Neville Granodiorite|64580|6|Mentioned|map legend|||||||||
22528|Neville Granodiorite|66845|4|Described|p537 Fig.3, p539 Tb.1, p540|||1861+/-12 Ma, single low U-zircon core SHRIMP analysis (no. 95.2).|magmatic crystallis'n age 1860+/-3 Ma SHRIMP U-Pb|Paperbark supersuite|||biotite granodiorite|
22528|Neville Granodiorite|66846|5|Briefly described|p558 Table 4|Orosirian|Orosirian|Age probably from U-Pb SHRIMP dating of zircon (see p547). |~1860 Ma|Of Paperbark supersuite.||||
22528|Neville Granodiorite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Data from OZCHRON1. Original comment: 'This igneous crystallisation age for the granite is based on 12 concordant data points'.|1860+/-3 Ma U/Pb SHRIMP|Paperbark Supersuite|||Medium- to fine-grained, biotite granodiorite and tonalite; minor monzogranite; abundant inclusions of metasedimentary rock at contact with Marboo Formation.|03-AUG-15
22528|Neville Granodiorite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv. |1860 Ma|Paperbark Supersuite|||Medium- to fine-grained, biotite granodiorite and tonalite; minor monzogranite; abundant inclusions of metasedimentary rock at contact with Marboo Formation.|
22528|Neville Granodiorite|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|1860-1860 Ma (Isotopic)|Unit of Paperbark Supersuite.|||Medium- to fine-grained, biotite granodiorite and tonalite; minor monzogranite; abundant inclusions of metasedimentary rock at contact with Marboo Formation|
22528|Neville Granodiorite|70154|6|Mentioned|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv.|1860 Ma|Paperbark Supersuite||||
22528|Neville Granodiorite|71267|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (183 -1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1860+\-3 Ma (isotopic)|Unit of Paperbark Supersuite.|||Medium- to fine-grained, biotite granodiorite and tonalite; minor monzogranite; abundant inclusions of metasedimentary rock at contact with Marboo Formation|
22528|Neville Granodiorite|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen, North Australian Craton.|1860 +/- 3 Ma.|Paperbark Supersuite.|||Medium- to fine-grained, biotite granodiorite and tonalite; minor monzogranite; abundant inclusions of metasedimentary rock at contact with Marboo Formation.|
22528|Neville Granodiorite|72437|5|Briefly described|p13, p78-80|Palaeoproterozoic|Palaeoproterozoic|Lamboo Complex. Several samples and their analyses are provided.|c. 1860 Ma||||Granodiorite, biotite granodiorite, biotite monzodiorite, tonalite.|
80126|New Holland Sandstone|71212|5|Briefly described|p171-p175, p178, p250|||Local name. Hosts the Genesis-New Holland gold deposit. 20-80m thick, striking 70-80 degrees west with a strike extent exceeding 1500m. Contains bedding features such as trough cross-bedding and ripple marks. See also  p65, 66App.G p19, and also New Holland East Sandstone App.G p21.|||||Medium to very coarse-grained, locally pebbly to cobbly quartzofeldspathic sandstone.|26-SEP-17
35665|Newtown Felsic Volcanics|23137|4|Described|p245 Table.2|||||||||
36892|Ngangganawili conglomerate|23586|5|Briefly described|p17|||Informal name.||||||
36892|Ngangganawili conglomerate|23759|6|Mentioned|p17|||Informal.||||||
75378|Ngarrutji Monzogranite|66116|5|Briefly described|Map legend|Archean|Archean|Yilgarn Craton. 2659 +/- 8 Ma. Medium- to coarse-grained monzogranite with biotite and local hornblende; minor granodiorite; local pegmatite; metamorphosed.||||||
75378|Ngarrutji Monzogranite|66121|5|Briefly described|Map legend|Archean|Archean|Yilgarn Craton. c.2666 Ma. Medium- to coarse-grained monzogranite with biotite and local hornblende; minor granodiorite; local pegmatite; metamorphosed.||||||
75378|Ngarrutji Monzogranite|68107|5|Briefly described|p607 Fig.3, p609 Tb.1, p616.|Neoarchean|Neoarchean|Burtville Terrane. Emplaced during later stages of folding and shearing of the Mount Venn Greenstone Belt; similar age to Point Salvation Monzogranite.|2666 +/- 8 Ma (Wingate et al. 2009).||||Granite.|22-SEP-14
75378|Ngarrutji Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||Includes one unnamed subunit.||Medium- to coarse-grained monzogranite with biotite and local hornblende; minor granodiorite and local pegmatite; medium- to coarse-grained monzogranite with xenoliths of mafic intrusive rock and minor felsic volcanic rocks; metamorphosed.|06-AUG-15
75378|Ngarrutji Monzogranite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|See also 100k_geologyp14_lut.csv and 500k_interpgeop14_lut.csv. Age derived from monzogranite sample (185972.1.pdf)|2666 +/- 8 Ma (SHRIMP)||||Medium- to coarse-grained monzogranite with biotite and local hornblende; minor granodiorite and local pegmatite. Medium- to coarse-grained monzogranite with xenoliths of mafic intrusive rock and minor felsic volcanic rocks; both are metamorphosed.|
75378|Ngarrutji Monzogranite|70802|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism.|2666+\-8 Ma||||Medium- to coarse-grained monzogranite with biotite and local hornblende; minor granodiorite and local pegmatite; metamorphosed|
75378|Ngarrutji Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 100k_geologyp14_lut.csv, 500k_interpgeop_lut.csv, 2_5m_interpgeop15_lut.csv.|2666+\-8 Ma||||Medium- to coarse-grained monzogranite with biotite and local hornblende; minor granodiorite and local pegmatite, contains xenoliths of mafic intrusive rock and minor felsic volcanic rocks; metamorphosed.|
75378|Ngarrutji Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||2666+/-8 Ma||||Medium- to coarse-grained monzogranite with biotite and local hornblende; minor granodiorite and local pegmatite; metamorphosed.|
74797|Ngumban Claystone Member|64502|3|Fully described|p766 Fig.3, p768 Fig.5, p 769, Fig.6||Early Permian|Of the Carolyn Formation, Grant Group, Lennard shelf region. Type section location given. Thickness 50m.Overlain by Deeadeea Sandstone Member. Contains dropstones from pebble to boulder size of granite, basalt, limestone.||||||27-JAN-10
74797|Ngumban Claystone Member|64643|4|Described|p18, 21|Sakmarian|Sakmarian|Of Carolyn Formation. Up to 50m thick.Type section in Deeadeea Cliffs. Overlain by Deeadeea Sandstone Member. Contains dropstones, up to boulder size, of granite, basalt, Proterozoic quartzite, Devonian limestone.||||||
74797|Ngumban Claystone Member|65486|4|Described|p18, 22, 24-25 Figs.25-26, 30-31, 55|Early Permian|Early Permian|Of basal Carolyn Formation. Sandy claystone with dropstones of granite, basalt, dolerite, quartzite, limestone; some faceted and striated. 50 m thick. Unconformably overlies Prices Creek Group, Fairfield Group. Underlies Deeadeea Sandstone Member.||||||
74797|Ngumban Claystone Member|66127|3|Fully described|pp213-214, pp283-286.|Early Permian|Early Permian|Of Playford (2002a). Named after Ngumban Cliff. Type section from the road cut on the Great Northern Highway to the top of Deeadeea Cliff. 50 m thick.||Lower unit in Carolyn Formation.||Unconformably overlies Pillara Limestone. Is overlain by Deeadeea Sandstone Member.|Contains pebble to boulder sized dropstones, some faceted and striated.|
74797|Ngumban Claystone Member|66949|4|Described|p10, p13-14, p16, p19, p57 Appx.3|Sakmarian|Sakmarian|See also p86 Appx.5. Restricted to easternmost Lennard Shelf. Outcropping type section detailed. Up to 40m thick; glacial lacustrine to ?lagoonal deposits.||Unit in Carolyn Formation.|||Siltstone with dropstones, minor sandstone.|02-NOV-15
78966|Niagara Igneous Complex|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2686 - 2600 Ma (inferred).||||Gabbronorite, dolerite, anorthositic gabbro, quartz diorite; metamorphosed.|
31105|Niagara Layered Complex|24196|6|Mentioned|p70|||Geological Province: West Malcolm sub-domain, Yilgarn Craton.||||||
31105|Niagara Layered Complex|43478|2|Defined|p33-61|||||||||
23873|Nibil Formation|14228|5|Briefly described|p6 fig3|Late Ordovician|Late Ordovician|South Canning Basin.||Carribuddy Group||Overlies Minjoo Salt. Overlain by Mallowa Salt.||06-OCT-16
23873|Nibil Formation|22753|5|Briefly described|Fig.3 p585|Ordovician|Ordovician|||||||
23873|Nibil Formation|24449|5|Briefly described|p741 Fig. 2|Ashgillian|Caradocian|Of Carribuddy Group. Geological Province: Canning Basin.||||||24-NOV-08
23873|Nibil Formation|40837|2|Defined|p257 Fig. 4, p273|Gedinnian|Gedinnian|Of the Carribuddy Group - replacing Unit C of Carribuddy Formation. See also Fig. 5 page insert (p258).||||||27-JAN-10
23873|Nibil Formation|42030|6|Mentioned|p746|||||||||
23873|Nibil Formation|43563|6|Mentioned|Fig.2,p5|||||||||
23873|Nibil Formation|43656|6|Mentioned|Fig.2,p8|Ashgillian|Caradocian|||||||
23873|Nibil Formation|43666|6|Mentioned|p49,Table 2||Ordovician|||||||
23873|Nibil Formation|43746|6|Mentioned|Fig.2,p11|Ashgillian|Caradocian|||||||
23873|Nibil Formation|43818|6|Mentioned|Fig.2.p39||Silurian|||||||06-OCT-16
23873|Nibil Formation|44143|4|Described|p.440 Table 4-19; p.442, Figure 4-96|Devonian|Silurian|Unit in Carribuddy Group. Up to 404m thick; claystone, dolomite & siltstone; sabkha and supratidal marine. Conformably overlies Minjoo Salt. Type section between 3501 and 3905m in Kidson 1 (URAL: 22deg 37' 27 " S, 125deg 00' 17" E). Contains sparse spores and pollen.||||||
23873|Nibil Formation|61021|5|Briefly described|p36 Fig. 2|Caradocian|Caradocian|Geological Province: Canning Basin.||||||17-DEC-07
23873|Nibil Formation|61551|5|Briefly described|p351 Fig.2, p359.|Late Ordovician|Late Ordovician|Canning Basin. Has excellent hydrocarbon source and seal potential.||Unit in Carribuddy Group.||Overlies Minjoo Salt. Is overlain by Mallowa Salt.|Shales.|
23873|Nibil Formation|64334|5|Briefly described|p39|Ordovician|Ordovician|Canning Basin; subsurface only. Caradoc-Ashgill.||Carribuddy Group.||Overlies Minjoo Salt and Mount Troy Formation. Is overlain by Mallowa Salt and Sahara Formation.|Mudstone.|
23873|Nibil Formation|64643|5|Briefly described|p3 Fig. 2|Upper Ordovician|Upper Ordovician|Of Carribuddy Group?||||||
23873|Nibil Formation|64982|5|Briefly described|p698.|Early Ordovician|Early Ordovician|Over 400 m of supratidal/playa lake deposits.||Unit in Carribuddy Group.||Overlies Minjoo Salt and Mount Troy Formation. Is overlain by Mallowa Salt.|Claystone, dolomite and siltstone.|
23873|Nibil Formation|65301|5|Briefly described|p5 Fig. 4, p8 Fig. 5|Late Ordovician|Late Ordovician|Geological province: Canning Basin.||||||
23873|Nibil Formation|65449|3|Fully described|p1, p6-11, p13-14, p17, p21-23, p37-38|Late Ordovician|Late Ordovician|See also p47-50, p54-57; Plates 1-5, 8-9, 11. Lehmann (1984), after Nibil Native Well. Defined as the predominantly non-evaporative interval between the Minjoo and Mallowa Salts. Type section is the interval 3905-3501m in Kidson 1. Contains a 5-10m thick sandstone marker unit from which oil shows have been reported. Age from surrounding units. Potential reservoir for Bongabinni Formation oil. Biostratigraphic data detailed.||Carribuddy Group.||Conformably overlies Minjoo Salt. Is overlain conformably by Mallowa Salt or Sahara Formation.|Grey, calcareous and less commonly dolomitic, mudstone locally grading to silty and argillaceous limestone and less commonly dolomite, with rare sandstone interbeds; minor halite; anhydrite is common.|
23873|Nibil Formation|68007|5|Briefly described|p11, Plate 1|Late Ordovician|Late Ordovician|Canning Basin.||Carribuddy Group.||Overlies Minjoo Salt. Is overlain by Mallowa Salt.||24-FEB-20
23873|Nibil Formation|68902|5|Briefly described|p9 fig 5|Ordovician|Ordovician |||Carribuddy Group||Overlies Minjoo Salt and Bongabinni Formation; overlain by Mallowa Salt and Sahara Formation.||
23873|Nibil Formation|69029|6|Mentioned|p319|Late Ordovician|Late Ordovician|Of Canning Basin.||||Overlain by Mallawo Salt. Underlain by Minjoo Salt.||
23873|Nibil Formation|69182|6|Mentioned|Ch4 p9-p12, Ch4 p40-p41|Late Ordovician|Late Ordovician|Canning Basin. See also Ch4 p44, Ch4 p45, Ch4 p47, Ch4 p50-p58, Ch4 p74, Ch4 p79-p82, Ch4 p92. ||Carribuddy Group||Overlies the Minjoo Salt and the Bongabinni Formation. Overlain by the Mallowa Salt and the Sahara Formation.|Sandstones and dolomites.|11-FEB-20
23873|Nibil Formation|69312|6|Mentioned|p3, p19, p24 fig 28|Late Ordovician|Late Ordovician|Canning Basin. See also  p25 fig 30, p27 fig 34, p28 fig 36. ||Carribuddy Group||Overlies the Minjoo Salt and the Mount Troy Formation. Overlain by the Mallowa Salt.|Shale.|11-FEB-20
23873|Nibil Formation|69883|6|Mentioned|p4-p5|Ashgill|Caradoc|Canning Basin. Supersequences provided.||Carribuddy Group||Overlies the Minjoo Salt and the Mount Troy Formation. Overlain by the Mallowa Salt.||
23873|Nibil Formation|70774|5|Briefly described|p4|Late Ordovician|Late Ordovician|Willara and Kidson Sub-basins, Canning Basin.||Carribuddy Group||Overlies the Bongabinni Formation and the Minjoo Salt. Overlain by the Mallowa Salt.||06-FEB-20
23873|Nibil Formation|71171|6|Mentioned|p2|||Canning Basin.||||||
23873|Nibil Formation|71870|5|Briefly described|p3|Katian|Katian|Canning Basin.||Carribuddy Group||Overlies the Minjoo Salt. Overlain by the Mallawa Salt.||
23873|Nibil Formation|71894|5|Briefly described|p4|Late Ordovician|Late Ordovician|Canning Basin.||Carribuddy Group||Overlies the Minjoo Salt. Overlain by the Mallowa Salt.|Shale.|11-FEB-20
23873|Nibil Formation|72497|5|Briefly described|p3 Fig.2.|Katian|Sandbian|Shown as occuring in the Anketell, Tabletop, Ryan Shelves, Willara and Kidson Sub-basins, the Jurgurra and Barbwire Terraces and Broome Platform. Age shown as upper Caradocian~= Eastonian (Aust), Katian (ICS).||Carribuddy Group||Conformably overlies Minjoo Salt and Mount Troy Formation and underlies Mallowa Salt.||
23873|Nibil Formation|72499|5|Briefly described|p7 Fig.6.|Late Ordovician|Late Ordovician|Located in the Willara Sub-basin and the Broome Platform.||Carribuddy Group||Overlies Minjoo Salt ?and Bongabinni Formation. and Underlies Mallowa Salt,?and Sahara Formation.|Includes shale.|
23873|Nibil Formation|73117|5|Briefly described|p3|Upper Ordovician|Upper Ordovician|Canning Basin.||Carribuddy Group||Underlain by Minjoo Salt. Overlain by Mallowa Salt.|Dominantly shale and mudstone.|
23873|Nibil Formation|73344|6|Mentioned|p6|Katian|Sandbian|Canning Basin, subsurface. Part of supersequence B1.||Carribuddy Group||Underlain by Minjoo Salt / Mount Troy Formation. Overlain by Mallowa Salt.||
23873|Nibil Formation|73346|6|Mentioned|p18, p27|Katian|Katian|Canning Basin. Includes the arandaspid Ritchieichthys nibili; provides biostratigraphic age constraint.||Carribuddy Group||||
80139|Nilemah Sand|69558|4|Described|p24,p113, p95, p105, p190 fig 295, p239|Holocene|Late Pleistocene|Originally the 'Nilemah Sands' of Logan et al (1970b). Named for the abandoned Nilemah Homestead. Probably formed from the leaching of Tamala Limestone and Peron Sandstone. Variably contains heavy minerals including ilmenite, zircon and rutile that form an orebody known as the Coburn heavy mineral sands or the 'Amy Zone'.|||||Red sand. Grading from, sandy calcarenite adjoining the coast to quartz sand further inland.|26-MAY-21
26808|Nilling Formation|24410|5|Briefly described|p134 Fig. 79|Proterozoic|Proterozoic|Siltstone, shale, sandstone and dolomite.||||||
26808|Nilling Formation|24526|5|Briefly described|p112 Fig. 9|Neoproterozoic|Neoproterozoic|Composed of folded greywacke and sandstone.  Age: >800Ma.  See also p114.||||||
26808|Nilling Formation|24542|5|Briefly described|p2 Fig.2, p12|Proterozoic|Proterozoic|Greywacke and sandstone.||||||
26808|Nilling Formation|38998|4|Described|p11|||||||||
26808|Nilling Formation|40340|5|Briefly described|p7|||||||||
26808|Nilling Formation|40341|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Middle to Late||||||
26808|Nilling Formation|40343|6|Mentioned|p10|||||||||
26808|Nilling Formation|41271|6|Mentioned|p21|||||||||
26808|Nilling Formation|44138|5|Briefly described|p264 Fig.3-54, p265, p272|||Deformed, low-grade metasedimentary rocks.|||||Thin-bedded quartz greywacke and sandstone, deformed and metamorphosed.|
26808|Nilling Formation|64580|4|Described|map legend||Mesoproterozoic|Fine- to very coarse-grained sandstone; variably pebbly, micaceous and silty.||||||09-DEC-08
26808|Nilling Formation|64722|6|Mentioned|Fig. 9 p. 19|Proterozoic|Proterozoic|Yilgarn margin.||||||11-APR-12
26808|Nilling Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, shale, sandstone, crystalline dolostone/dolomite|
26808|Nilling Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Badgeradda Basin.|||||Fine- to very coarse-grained sandstone; variably pebbly, micaceous and silty.|
78591|Nindibillup Dyke Suite|65487|4|Described|p5-7, 9, p8 Fig. 3, p25-26 Fig. 13-14|||New name. Cuts the southern part of the Southern Cross Domain and Southwest Terrane of the South Yilgarn Craton. E-SE trending. Strongly magnetic to non-magnetic; Age unknown but may correlate with Early Cambrian dykes in the western Albany-Fraser Orogen. Mafic. Composition largely unknown.||||||16-JAN-14
78591|Nindibillup Dyke Suite|68186|5|Briefly described|p29-31, Plate 1A|Phanerozoic|Proterozoic|N of Esperance. ESE-trending dykes, varying from nonmagnetic to strongly magnetic and hundreds of kilometres long. Post-dates Stage II (1215-1140 Ma) of the Albany-Fraser Orogeny.|c.750 Ma.||||Dolerite dykes, WNW-trending, variably magnetic. Some exceeding 400km long. Mostly interpreted from aeromagnetic data.|
78591|Nindibillup Dyke Suite|69003|6|Mentioned|p4|||Albany-Fraser Orogen.||||||
78591|Nindibillup Dyke Suite|69412|6|Mentioned|p3 Fig.2, p7|||Ravensthorpe area, Yilgarn Craton. SE- and ESE-trending dykes.|c.750 Ma.|||||
78591|Nindibillup Dyke Suite|70023|6|Mentioned|p170|||Eastern Nornalup Zone and Madura Province.||||||
78591|Nindibillup Dyke Suite|70794|5|Briefly described|2_5m_interpdykel15_lut.csv|Cryogenian|Tonian|West-northwesterly trending, variably magnetic; some exceeding 400 km in length; mostly interpreted from aeromagnetic data. |800-700 inferred.||||Mafic dykes.|
78591|Nindibillup Dyke Suite|70802|5|Briefly described|GEOL_LUT_CSV files|Cryogenian|Tonian|Geological province: Albany-Fraser Orogen. Events: Western Australian events (4000-0.01 Ma). See 2_5m_interpdykel15_lut.csv, 250k_pre_mesozoic_interpgeol_lut.csv.|800-700 Ma (inferred)||||Mafic dykes; west-northwesterly trending, variably magnetic; some exceeding 400 km in length; mostly interpreted from aeromagnetic data|
78591|Nindibillup Dyke Suite|70826|6|Mentioned|p14 tbl 5|Cryogenian|Cryogenian|South-east Yilgarn, Albany Fraser Orogen.|800-700 Ma|||||
78591|Nindibillup Dyke Suite|71270|4|Described|2_5m_interpdykel15_lut.csv|Cryogenian|Tonian|Geological province: Yilgarn Craton, West Australian Craton. Events: Western Australian events (4000 - 0.01 Ma).|800-700 Ma (inferred)||||Mafic dykes; west-northwesterly trending, variably magnetic; some exceeding 400 km in length; mostly interpreted from aeromagnetic data|
80968|Ninety Seven Mile Formation and Elimberrie Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoproterozoic|Neoproterozoic|Oscar Range Sub-basin, Louisa Basin. Informal grouping of units suitable for map scale.|||||Sandstone, diamictite, siltstone, limestone, phyllite, quartzite, metabasalt, metatuff, and metarhyolite.|
79001|Ninghan Gabbro|70830|5|Briefly described|p57|||This unit is up to 500m thick.||Warriedar Suite||||
79001|Ninghan Gabbro|71809|5|Briefly described|map legend|Archean|Archean|Yilgarn Craton||Of Warriedar Suite.|||Gabbro, gabbronorite and dolerite; pegmatitic leucogabbro in top contact zones of sills, and pyroxenite and minor peridotite at the base; metamorphosed.|
79739|Nobb Well Intrusion|60429|2|Defined|p13,  p36 Appdx. 1|Archean|Archean|Small concordant ultramafic body - coarse-grained, serpentinised peridotite, minor metapyroxenite.Occurs along contact between Duffer Fm and overlying Apex Basalt. Intruded by Mullugunya Granodiorite. Age: c.3471-3300Ma. Max. thickness: ~600m.||||||
25346|Nome Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p221 Fig. 15|Late Triassic|Late Triassic|Of Sahul Group. In figure, Fm = Formation. Geological Province: Bonaparte Basin.||||||01-MAR-10
25346|Nome Formation|7142|6|Mentioned|p350 Fig.4.|Early Jurassic|Late Triassic|Browse Basin.||||Overlies Challis Formation. Is overlain by Plover Formation.||
25346|Nome Formation|13194|4|Described|p386 Tb. 4-16|Norian|Carnian|Type Section: Jabiru 1A well (1887-2184m). Up to 500m thick deltaic deposits.||Sahul Group||Overlies Challis Formation. Coeval with Benalla Formation.|Interbedded sandstone, siltstone and shale; minor coal.|
25346|Nome Formation|13222|6|Mentioned|p229 Fig.2.|||||Unit in Sahul Group.||||
25346|Nome Formation|13354|6|Mentioned|p375 Fig.6, p376 Fig.7.|Early Jurassic|Late Triassic|Bonaparte Basin. Unit of Sahul Group. Overlies Challis Formation and underlies Plover Formation.||96||||28-OCT-14
25346|Nome Formation|22663|5|Briefly described|AC97 1-4 Fig.4||Late Triassic|Of the Sahul Group.||||||01-MAR-10
25346|Nome Formation|23378|6|Mentioned|p180 Fig.2||Late Triassic|Of the Sahul Group.  In the Vulcan Sub-basin.||||||21-NOV-06
25346|Nome Formation|24171|5|Briefly described|p722 Fig. 3|Triassic|Triassic|Geological Province : Vulcan Sub-Basin.||||||01-MAR-10
25346|Nome Formation|24207|5|Briefly described|p209 Fig. 5|Late Triassic|Late Triassic|||||||01-MAR-10
25346|Nome Formation|24427|5|Briefly described|p49 Fig.2||Triassic|Geological Province: Bonaparte Basin.||||||
25346|Nome Formation|41532|2|Defined|p302|Late Triassic||||||||
25346|Nome Formation|42053|5|Briefly described|Fig.2 P29|||||||||01-MAR-10
25346|Nome Formation|42066|6|Mentioned|Fig.3 P199|||||||||
25346|Nome Formation|42442|2|Defined|p22|Norian|Carnian|Variation of Nome Formation, WA.||||||
25346|Nome Formation|43826|6|Mentioned|Fig.2,p163||Late Triassic|||||||01-MAR-10
25346|Nome Formation|60634|6|Mentioned|p1168 Fig.3. |Early Jurassic|Late Triassic|||Unit in Sahul Group.||Overlies Challis Formation. Is overlain by Plover Formation.||
25346|Nome Formation|61548|6|Mentioned|p480 Fig.3|Late Triassic|Late Triassic|Northern Bonaparte Basin.||||||
25346|Nome Formation|61550|6|Mentioned|p495 Fig.2. |Late Triassic|Late Triassic|||Unit in Sahul Group.||Overlies Challis Formation.||
25346|Nome Formation|62837|5|Briefly described|Stratigraphic columns|Early Jurassic|Late Triassic|Of the Sahul Group.  Age: ~213-~203Ma. Geological Province:  Vulcan Sub-basin (Western Bonaparte Basin).||||||01-MAR-10
25346|Nome Formation|63358|5|Briefly described|p4 Fig. 1.3, p152++|Hettangian|Norian|||||||01-MAR-10
25346|Nome Formation|63929|6|Mentioned|p131 Fig.2.|Late Triassic|Late Triassic|Ashmore Platform (east), Sahul Platform. Includes marine and non-marine, with local red beds, sediments.||||Overlies Challis Formation. Is overlain by Malita Formation.||
25346|Nome Formation|64689|5|Briefly described|p7 Fig.6|Late Triassic|Late Triassic|Rhaetian.||||Overlies Challis Formation. Is overlain unconformably by Plover Formation.||20-SEP-14
25346|Nome Formation|64693|6|Mentioned|p375|Triassic|Triassic|||||Unconformably overlies Challis Formation.||
25346|Nome Formation|64696|6|Mentioned|p127 Fig.2 |Rhaetian|Rhaetian|||||Is overlain unconformably by Plover Formation.||
25346|Nome Formation|64697|5|Briefly described|p84 Fig.2 |Late Triassic|Late Triassic|||||||
25346|Nome Formation|66124|5|Briefly described|p171 Fig.2|Norian|Rhaetian|Ashmore Platform (East). Marine; contains conodonts. Underlies Malita Formation and overlies Challis Formation.||||||
25346|Nome Formation|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Rhaetian|Norain|Sahul Group. Underlies the Plover Formation, overlies the Challis Formation. Mount Ashmore Dome. Mixed shallow marine to deltaic sandstone and claystone with minor shallow-marine limestone.||||||
25346|Nome Formation|67195|5|Briefly described|Appendix 2|||Browse Basin.|||||Includes dark grey siltstone; highly fractured (healed? Doubtful drilling induced?)|23-DEC-22
25346|Nome Formation|67200|6|Mentioned|app 2 p7||||||||Siltstone.|
25346|Nome Formation|68223|6|Mentioned|p178 Fig.3|Norian|Norian|||||||
25346|Nome Formation|69297|6|Mentioned|p305|Rhaetian|Norian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin. ||Sahul Group||Overlies the Challis Formation. Overlain by the Ashmore Volcanics and the Plover Formation.|Sandstone and mudstone.|
25346|Nome Formation|69452|5|Briefly described|p36:15|Triassic|Triassic|Bonaparte Basin.||Sahul Group.||||12-JUL-16
25346|Nome Formation|69689|6|Mentioned|p16|Triassic|Triassic|Browse, Bonaparte Basins.||||Overlies Mount Goodwin Sub-group. Is overlain by Plover Formation.||
25346|Nome Formation|70061|5|Briefly described|Regional geology; Figs.6-7, p12|Rhaetian|Norian|See also Vulcan: Fig.2, p1-2. Hydrocarbon reservoir. Shallow marine sediments.||Sahul Group.||Overlies Challis Formation. Is overlain by Plover Formation.||12-JUL-16
25346|Nome Formation|70064|5|Briefly described|Regional Fig.6;p6,p8-9. Central: Fig.2|Rhaetian|Norian|See also Northern: Fig.2; p1-2. Yampi: Fig.2. Browse Basin. Potential reservoirs in horsts and tilted fault-blocks. Hosts gas (280m gas column) in the Crux structure within the Heywood Graben.||Sahul Group.||Overlies Challis Formation. Is overlain by Plover Formation or Ashmore Volcanics.|Relatively high-energy fluvial environment; includes quartz-rich, medium- to very coarse-grained sandstone with interbedded siltstone, mudstone and minor coal.|12-JUL-16
34890|Nooloo Formation|22907|6|Mentioned|41|||||||||
34890|Nooloo Formation|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Of Tarcunyah Group, Officer Basin.||||||
34890|Nooloo Formation|23590|2|Defined|p13, p22 Appendix 2|||Age: <830 Ma (poor age constraints). Of Tarcunyah Group. Underlying unit Wongarlong Formation. Officer Basin. Max. thickness: >1000 m.||||||
34890|Nooloo Formation|23729|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Tarcunyah Group. Geological Province; Paterson Orogen.||||||
34890|Nooloo Formation|23730|4|Described|p12|Neoproterozoic|Neoproterozoic|Of Tarcunyah Group. Underlying unit Choorun Formation. Geological Province: Officer Basin.||||||
34890|Nooloo Formation|23760|4|Described|p29|Neoproterozoic|Neoproterozoic|Of Tarcunyah Group. Geological Province: Officer Basin.||||||
34890|Nooloo Formation|50008|5|Briefly described|p46 Fig.3||Neoproterozoic|Of Tarcunyah Group. Geological Province: Officer Basin.||||||
34890|Nooloo Formation|60470|5|Briefly described|p4 Fig. 2|Neoproterozoic|Neoproterozoic|in Officer Basin, of Tarcunyah Group. Dolomite, siltstone, and shale||||||
34890|Nooloo Formation|62453|4|Described|p5 Fig. 3, 66|Cryogenian|Cryogenian|Geological Province: Paterson Orogen. Conformably overlies: Choorun Formation, Wongarlong Formation. Dolomite, limestone, chert, shale, siltstone, sandstone, conglomerate.||||||
34890|Nooloo Formation|64580|6|Mentioned|map legend|||Of Tarcunyah Group.||||||15-DEC-08
34890|Nooloo Formation|64777|5|Briefly described|p3 Fig.4 |Neoproterozoic|Neoproterozoic|||Of the Tarcunyah Group|||Dolomite, siltstone and shale.|
34890|Nooloo Formation|65403|6|Mentioned|p13.|||Facies equivalent of Waters Sandstone (?and Gunanya Sandstone).||Unit in Tarcunyah Group.||||
34890|Nooloo Formation|65454|4|Described|p7 Fig.3, p10, p30 Fig.A1b|Cryogenian|Cryogenian|Of Tarcunyah Group. Wide range of rock types ranging from fine- to coarse-grained sandstone, siltstone and shale, through to thinly bedded carbonate. Overlies Choorun Formation.||||||
34890|Nooloo Formation|65826|6|Mentioned|p7 Fig.4. |Neoproterozoic|Neoproterozoic|Officer Basin.||Unit in Tarcunyah Group.||||
34890|Nooloo Formation|67202|5|Briefly described|p64-65, p231|Neoproterozoic|Neoproterozoic|NW Officer Basin. Thickness unknown. Deep-water shelf deposits.||Topmost Tarcunyah Group.||Overlies Wongarlong Formation conformably, and Choorun Formation.|Thinly bedded dolomite and limestone, calcareous shale and siltstone.|
34890|Nooloo Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|NW Paterson Orogen.||Tarcunyah Group.||||
34890|Nooloo Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|Neoproterozoic|Neoproterozoic|||Unit of Tarcunyah Group.||||
34890|Nooloo Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||crystalline dolostone/dolomite, limestone, sandstone, siltstone|
34890|Nooloo Formation|72034|5|Briefly described|500k_interpgeop16_lut|Cryogenian|Tonian|Gibson Sub-basin, Officer Basin (Phase 1).||Tarcunyah Group|||Thinly bedded dolomite, limestone, shale, and sandstone.|
25347|Noondeening Orthogneiss|38513|6|Mentioned|Table II|||||||||
79286|Noongal Gabbro|70226|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Carton. Fifteen un-named facies are mapped separately.|2801-2793 Ma Warridar Suite|Warriedar Suite.|||Gabbro and dolerite; metamorphosed. Also, leucogabbro, serpentinite and tremolite-rich ultramafic schist (derived from intrusive rocks), metapyroxenite and metaperidotite.|16-DEC-15
79286|Noongal Gabbro|70796|5|Briefly described|100k_geologyp_lut.csv|Neoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_interpgeop_lut.csv,  500k_interpgeop_lut.csv.|ca 2801 to 2793 Ma (inferred)|Warriedar Suite|||Amphibolitic metagabbro and metadolerite with sheets of granitic to granodioritic schist; Metadolerite with lesser metagabbro, plagioclaseporphyritic gabbro, leucogabbro, plagioclaseporphyritic dolerite, metapyroxenite and lesser metaperidotite.|
79286|Noongal Gabbro|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.|2801-2793 Ma (inferred)|Unit of Warriedar Suite.|||Amphibolitic metagabbro and metadolerite: abundant sheets of granitic to granodioritic schist; metagabbro, locally hornblende-rich; plagioclase-porphyritic gabbro and dolerite, leucogabbro; locally  pegmatitic; metapyroxenite and metaperidotite.|
26080|Noonkanbah Formation|7433|5|Briefly described|p25 Fig.2, p32 Fig.8, pp36-37, pp52-53.|Permian|Permian|Canning Basin. Fine marine clastics. ||||Overlies Poole Sandstone. Is overlain by Triwhite Sandstone and Lightjack Formation.|Shale, siltstone; minor fine-grained, laminated to thin-bedded, calcareous marine units with minor coquinas of Neochonetes; minor cross-bedded bioclastic limestones; local phosphatic oolitic and massive ochreous ironstone. Richly fossiliferous.|
26080|Noonkanbah Formation|12733|6|Mentioned|p565.|Early Permian|Early Permian|Canning Basin.  Gas-prone.||||||
26080|Noonkanbah Formation|13255|6|Mentioned|p369|Permian|Permian|Roebuck Basin. Early Permian.||||Overlies Poole Sandstone. Is overlain by Liveringa Group.||
26080|Noonkanbah Formation|13354|6|Mentioned|p376 Fig.7.|Early Permian|Early Permian|Onshore Canning Basin. Overlies Poole Sandstone and underlies Liveringa Group.||78||||28-OCT-14
26080|Noonkanbah Formation|22718|5|Briefly described|p5, Table1 p7||Artinskian|||||||17-MAR-20
26080|Noonkanbah Formation|22738|4|Described|10,13,16, map|Early Permian|Early Permian|Max thickness 110 m. Overlain by Wallal Sandstone; underlain by Poole Sandstone.||||||13-NOV-07
26080|Noonkanbah Formation|22741|5|Briefly described|p28, Table3 p13||Artinskian|||||||17-MAR-20
26080|Noonkanbah Formation|22753|5|Briefly described|Fig.3 p585|Permian|Permian|||||||
26080|Noonkanbah Formation|22764|6|Mentioned|Table2,p10||Early Permian|300 M. Conformable on Poole Sandstone; conformable beneath Lightjack Formation||||||01-FEB-10
26080|Noonkanbah Formation|22765|5|Briefly described|p10, Table1||Artinskian|Maximum thickness is 76m, Overlain by Wallal Sandstone.||||||17-MAR-20
26080|Noonkanbah Formation|22767|5|Briefly described|Table3 p16, p22||Early Permian|||||||17-MAR-20
26080|Noonkanbah Formation|22776|4|Described|Table.3||Artinskian|see also p19.||||||
26080|Noonkanbah Formation|22801|5|Briefly described|p11, Table1 p9||Artinskian|||||||17-MAR-20
26080|Noonkanbah Formation|22814|5|Briefly described|fig2|Permian|Permian|||||||
26080|Noonkanbah Formation|23212|4|Described|Table.1 p7||Artinskian|||||||
26080|Noonkanbah Formation|23523|5|Briefly described|p994 Fig. 2|Permian|Permian|||||||
26080|Noonkanbah Formation|23765|5|Briefly described|Map Legend|Permian|Permian|||||||
26080|Noonkanbah Formation|23766|4|Described|p14 Tb. 2|Early Permian|Early Permian|Consists of siltstone, limestone and sandstone. Thickness: 540m.  See also p20.||||||13-NOV-07
26080|Noonkanbah Formation|24061|4|Described|p182|Early Permian|Early Permian|Geological Province:  Canning Basin.||||||
26080|Noonkanbah Formation|24062|5|Briefly described|p186 Table 1|Permian|Permian|Geological Province: Canning Basin.||||||
26080|Noonkanbah Formation|24160|4|Described|p45|Permian|Permian|||||Is conformably overlain by Hardman Formation.|Grey micaceous mudstone with interbedded calcareous sandstone.|
26080|Noonkanbah Formation|24246|5|Briefly described|p15|Permian|Permian|Geological Province: Canning Basin.||||||
26080|Noonkanbah Formation|24390|5|Briefly described|p6 Fig. 4|Permian|Permian|Geological Province: Canning Basin.  See also p8.||||||
26080|Noonkanbah Formation|24466|5|Briefly described|p368 Fig. 3|Permian|Permian|||||||
26080|Noonkanbah Formation|24552|5|Briefly described|p93, 95|||Contains bryozoans - species given. Geological Province: Fitzroy Basin and/or Canning Basin. WA||||||07-FEB-11
26080|Noonkanbah Formation|29548|6|Mentioned|p224|||Permian||||||
26080|Noonkanbah Formation|29813|6|Mentioned|p17|||||||||
26080|Noonkanbah Formation|29817|5|Briefly described|p8|||||||||
26080|Noonkanbah Formation|29818|6|Mentioned|Map legend|Permian|Permian|||||||
26080|Noonkanbah Formation|29819|6|Mentioned|Map legend|Permian|Permian|||||||
26080|Noonkanbah Formation|30110|6|Mentioned|p81|||See also P83. Lower Permian, Artinskian age.||||||
26080|Noonkanbah Formation|30313|4|Described|p54|||See also p55. Lower Permian age||||||13-NOV-07
26080|Noonkanbah Formation|30338|6|Mentioned|p100|||||||||
26080|Noonkanbah Formation|30342|6|Mentioned|Table 20|||||||||
26080|Noonkanbah Formation|30449|6|Mentioned|p11|||Brachiopods [Originally entered for Qld. CEBMar95]||||||
26080|Noonkanbah Formation|30525|6|Mentioned|Map legend|Artinskian|Artinskian|||||||
26080|Noonkanbah Formation|30533|4|Described|p25|||On Table 7.||||||13-NOV-07
26080|Noonkanbah Formation|30545|6|Mentioned|Fig.2|||Artinskian||||||
26080|Noonkanbah Formation|30550|6|Mentioned|p78|||Lower Permian age||||||
26080|Noonkanbah Formation|30595|5|Briefly described|p4|||||||||
26080|Noonkanbah Formation|30897|6|Mentioned|p19|||Refers Guppy et al.(1958)||||||
26080|Noonkanbah Formation|31396|6|Mentioned|p1183|||||||||
26080|Noonkanbah Formation|31598|6|Mentioned|p36|||||||||
26080|Noonkanbah Formation|31706|6|Mentioned|p657|||Permian correlation chart||||||
26080|Noonkanbah Formation|32648|6|Mentioned|p32|||L.Permian||||||
26080|Noonkanbah Formation|32945|6|Mentioned|p88|||Permian. See also P89||||||
26080|Noonkanbah Formation|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
26080|Noonkanbah Formation|33518|4|Described|p8|||||||||
26080|Noonkanbah Formation|33519|6|Mentioned|Map legend|Permian|Permian|||||||
26080|Noonkanbah Formation|33701|6|Mentioned|Fig.1|||Artinskian.||||||
26080|Noonkanbah Formation|33960|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26080|Noonkanbah Formation|33965|4|Described|Table 1|||||||||
26080|Noonkanbah Formation|33966|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26080|Noonkanbah Formation|34008|6|Mentioned|p69|||Permian||||||
26080|Noonkanbah Formation|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
26080|Noonkanbah Formation|34287|6|Mentioned|p125|||||||||
26080|Noonkanbah Formation|34345|5|Briefly described|p329|||Affinities with overseas formations. See also p330.||||||13-NOV-07
26080|Noonkanbah Formation|34532|6|Mentioned|p224|||See also PP225-228||||||
26080|Noonkanbah Formation|35120|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26080|Noonkanbah Formation|35124|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26080|Noonkanbah Formation|35127|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26080|Noonkanbah Formation|35201|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26080|Noonkanbah Formation|35202|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26080|Noonkanbah Formation|35205|6|Mentioned|Map legend|Permian|Permian|||||||
26080|Noonkanbah Formation|35207|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26080|Noonkanbah Formation|35222|4|Described|Table.2|||||||||
26080|Noonkanbah Formation|35223|4|Described|Table.2|||||||||
26080|Noonkanbah Formation|35225|4|Described|Table 1|||||||||
26080|Noonkanbah Formation|35226|4|Described|Table 1|||||||||
26080|Noonkanbah Formation|35250|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26080|Noonkanbah Formation|35251|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26080|Noonkanbah Formation|35252|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26080|Noonkanbah Formation|35275|6|Mentioned|Fig.5.|||||||||
26080|Noonkanbah Formation|35497|4|Described|Table 1|||Also on p10.||||||13-NOV-07
26080|Noonkanbah Formation|35530|6|Mentioned|p2|||Location of Bivalvia fossils.||||||
26080|Noonkanbah Formation|35903|4|Described|Table 1|||||||||
26080|Noonkanbah Formation|35983|6|Mentioned|Table 28|||||||||
26080|Noonkanbah Formation|36020|6|Mentioned|p392|||||||||
26080|Noonkanbah Formation|36224|5|Briefly described|Map legend|Early Permian|Early Permian|Mudstone, calcareous, micaceous; limestone, fine sandstone interbeds; minor granule conglomerate lenses; fossiliferous.||||||01-FEB-05
26080|Noonkanbah Formation|36225|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26080|Noonkanbah Formation|36257|6|Mentioned|Table 2.1|||||||||
26080|Noonkanbah Formation|36438|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26080|Noonkanbah Formation|36632|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26080|Noonkanbah Formation|36634|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26080|Noonkanbah Formation|36890|3|Fully described|p341|||Formerly Noonkanbah Series.||||||13-NOV-07
26080|Noonkanbah Formation|37106|5|Briefly described|p277|||||||||
26080|Noonkanbah Formation|37369|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26080|Noonkanbah Formation|37370|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26080|Noonkanbah Formation|37549|6|Mentioned|p109|||||||||
26080|Noonkanbah Formation|37812|6|Mentioned|p653|||||||||
26080|Noonkanbah Formation|38444|6|Mentioned|p300|||||||||
26080|Noonkanbah Formation|38603|6|Mentioned|p81|||||||||
26080|Noonkanbah Formation|38878|6|Mentioned|Map legend|Artinskian|Artinskian|||||||
26080|Noonkanbah Formation|38886|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26080|Noonkanbah Formation|39169|6|Mentioned|p73|||||||||
26080|Noonkanbah Formation|39223|6|Mentioned|p238|||||||||
26080|Noonkanbah Formation|39796|6|Mentioned|Map legend|Permian|Permian|||||||
26080|Noonkanbah Formation|39857|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26080|Noonkanbah Formation|39974|6|Mentioned|p113|||||||||
26080|Noonkanbah Formation|40045|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26080|Noonkanbah Formation|40078|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26080|Noonkanbah Formation|40838|6|Mentioned|p281|||||||||
26080|Noonkanbah Formation|40992|6|Mentioned|Fig.11|||||||||
26080|Noonkanbah Formation|41044|6|Mentioned|p137|||||||||
26080|Noonkanbah Formation|41049|6|Mentioned|p39|||||||||
26080|Noonkanbah Formation|41071|6|Mentioned|p25|||||||||
26080|Noonkanbah Formation|41100|6|Mentioned|p288|||||||||
26080|Noonkanbah Formation|41158|6|Mentioned|p80|||See also P189||||||
26080|Noonkanbah Formation|41169|6|Mentioned|p148|||||||||
26080|Noonkanbah Formation|41215|6|Mentioned|p281|||||||||
26080|Noonkanbah Formation|41514|6|Mentioned|p81|||||||||
26080|Noonkanbah Formation|41639|6|Mentioned|p14|||||||||
26080|Noonkanbah Formation|41666|6|Mentioned|p10|||||||||
26080|Noonkanbah Formation|41688|6|Mentioned|p10|||||||||
26080|Noonkanbah Formation|41689|6|Mentioned|Table 1|||||||||
26080|Noonkanbah Formation|41730|6|Mentioned|p483|||||||||
26080|Noonkanbah Formation|41809|6|Mentioned|p68|||||||||
26080|Noonkanbah Formation|42347|6|Mentioned|Fig.2 p1020|||||||||17-MAR-20
26080|Noonkanbah Formation|42392|6|Mentioned|p115|||Member of Holmwood Shale||||||
26080|Noonkanbah Formation|42462|6|Mentioned|p58|||Canning Basin||||||
26080|Noonkanbah Formation|42540|6|Mentioned|p311|||Canning Basin||||||
26080|Noonkanbah Formation|42571|5|Briefly described|p20, Table1 p9|||||||||
26080|Noonkanbah Formation|42613|6|Mentioned|p16|||includes "Dora Shale".||||||17-MAR-20
26080|Noonkanbah Formation|42654|6|Mentioned|p10|||||||||
26080|Noonkanbah Formation|42710|5|Briefly described|map legend|Permian||||||||
26080|Noonkanbah Formation|42811|5|Briefly described|p44|||||||||
26080|Noonkanbah Formation|42880|5|Briefly described|Fig.2,p1020|||||||||
26080|Noonkanbah Formation|42930|5|Briefly described|Fig.1 p473|Permian|Permian|Age is Middle Permian. Unconformably overlies Poole Sandstone; conformably overlain by Liveringa Formation. Geological Province: Canning Basin.||||||13-NOV-07
26080|Noonkanbah Formation|42994|5|Briefly described|p36|||||||||
26080|Noonkanbah Formation|43015|5|Briefly described|Table 1,p319|||||||||
26080|Noonkanbah Formation|43018|5|Briefly described|Table 1,p386|||||||||
26080|Noonkanbah Formation|43050|5|Briefly described|p6|||||||||
26080|Noonkanbah Formation|43173|5|Briefly described|12-54||Early Permian|||||||
26080|Noonkanbah Formation|43281|5|Briefly described|Map legend||Permian|||||||
26080|Noonkanbah Formation|43563|6|Mentioned|Fig.2,p5|Kungurian|Artinskian|||||||
26080|Noonkanbah Formation|43656|6|Mentioned|Fig.2,p8|Kungurian|Artinskian|||||||
26080|Noonkanbah Formation|43737|6|Mentioned|p5||Kungurian|||||||
26080|Noonkanbah Formation|43746|6|Mentioned|Fig.2,p11|Kungurian|Artinskian|||||||
26080|Noonkanbah Formation|43818|6|Mentioned|Fig.2.p39||Early Permian|||||||
26080|Noonkanbah Formation|43932|5|Briefly described|p8,Tb.1 p6||Permian|||||||
26080|Noonkanbah Formation|44040|14|Not recorded|p41-43|||||||||
26080|Noonkanbah Formation|44143|4|Described|p436 Table 4-19, p445, p446 Figure 4-102|Permian|Permian|Up to 500m thick; mudstone interbedded with sandstone; marine. Conformably overlies Poole Sandstone and is overlain conformably by Triwhite Sandstone or Lightjack Formation. Type section near Bruten Hill (NOONKANBAH: 18deg 44' 35" S, 125deg 37' 30" E). Contains brachiopods, bryozoans, corals, crinoids and molluscs; Artinskian.||||||24-NOV-17
26080|Noonkanbah Formation|44219|14|Not recorded|p31||Artinskian|||||||
26080|Noonkanbah Formation|44231|5|Briefly described|Map Legend|Permian|Permian|Geological Province: Canning Basin.|||||Fine-grained calcareous sandstone, ferruginous sandstone, and shale; restricted marine|02-OCT-09
26080|Noonkanbah Formation|44344|14|Not recorded|p.14,15|||Eqiv. of Wandagee Formation; top of unit ?equiv. of Baker Formation. (G50-1).||||||
26080|Noonkanbah Formation|44356|5|Briefly described|p9,Tb.1 p6|||Artinskian palynomorphs.||||||
26080|Noonkanbah Formation|44357|4|Described|p12,Tb.1 p9||Artinskian|Subsurface only.||||||
26080|Noonkanbah Formation|44397|14|Not recorded|p.13,20, Table 4||Permian|Perm.||||||
26080|Noonkanbah Formation|44398|14|Not recorded|map legend||Permian|||||||
26080|Noonkanbah Formation|44403|2|Defined|opp.p6, Tb.1||Artinskian|E/51-12. Disconformably overlies Poole Sandstone and is conformably overlain by Liveringa Formation. Possible source rocks for petroleum. Some aquifers.||||||17-MAR-20
26080|Noonkanbah Formation|44404|14|Not recorded|map legend||Permian|||||||
26080|Noonkanbah Formation|44657|14|Not recorded|p.10|||||||||
26080|Noonkanbah Formation|44994|6|Mentioned|Fig.7|||Permian. Correlation.||||||
26080|Noonkanbah Formation|44998|2|Defined|p80|Kungurian|Artinskian|Overlies Grant Formation. See also p67,70-80,84-6,88-9,91-3,96,103,173-8,221-9,245-7,App.2 p266,267,App.4 p286.||||||17-MAR-20
26080|Noonkanbah Formation|45001|14|Not recorded|p7|Artinskian|Artinskian|||||||
26080|Noonkanbah Formation|45031|14|Not recorded|p22,31,36,37,54,56||Permian|||||||
26080|Noonkanbah Formation|45101|6|Mentioned|Fig.27|||||||||
26080|Noonkanbah Formation|45140|5|Briefly described|p64, p67|Permian|Permian|Marine deposits. Correlation with Lucas Formation was suggested by Casey and Wells (1964) but regarded in this study as dubious.||||Conformably overlies Poole Sandstone. Is overlain conformably by Lightjack Formation.|Mostly fossiliferous siltstone and shale.|
26080|Noonkanbah Formation|45143|6|Mentioned|p53|||||||||
26080|Noonkanbah Formation|45153|2|Defined|App.4-71|late Artinskian|late Artinskian|||||||
26080|Noonkanbah Formation|45158|3|Fully described|p20|||See also p11.||||||13-NOV-07
26080|Noonkanbah Formation|46849|6|Mentioned|p186|||||||||
26080|Noonkanbah Formation|46864|6|Mentioned|p40|||||||||
26080|Noonkanbah Formation|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
26080|Noonkanbah Formation|48573|2|Defined|p.3,8,11-13,21|||(E51-7/Alexander Creek)||||||
26080|Noonkanbah Formation|48596|14|Not recorded|p.5|||(E51-11)||||||
26080|Noonkanbah Formation|48826|14|Not recorded|p.22-4|||Tb.III, p.22-4,27-8,37,Pl.1. Correlates with Dora Shale. Grades into Balgo Member. Overlain by Blina Shale. (E51-13,F52-1,2,6).||||||
26080|Noonkanbah Formation|48831|14|Not recorded|p.31-35|||On many pages. p.8,9,11,12,15,17-19,22,24,25,31-35,37-41,52-58,63,65,68,69.||||||
26080|Noonkanbah Formation|48837|14|Not recorded|p.13|||On many pages. p.1,6,7,10,11,12,13,16.||||||
26080|Noonkanbah Formation|48848|14|Not recorded|36,38,47,51-58,64,74|||||||||
26080|Noonkanbah Formation|49644|5|Briefly described|Table|||||||||
26080|Noonkanbah Formation|50085|5|Briefly described|p6 Fig. 4|Permian|Permian|Geological Province: Canning Basin.||||||
26080|Noonkanbah Formation|60295|5|Briefly described|p132|||Geological Province: Carnarvon Basin||||||
26080|Noonkanbah Formation|60386|5|Briefly described|p297, 310|Kungurian|Artinskian|Roebuck/Canning Basin. Proximal shelf overlain by limestone nearshore-shelf.||||||
26080|Noonkanbah Formation|61021|5|Briefly described|p36 Fig. 2|Kungurian|Artkinsian|Geological Province: Canning Basin.||||||17-DEC-07
26080|Noonkanbah Formation|61023|5|Briefly described|p10 Fig. 6|Permian|Permian|Geological Province: Canning Basin.||||||11-APR-08
26080|Noonkanbah Formation|61551|6|Mentioned|p351 Fig.2. |Kungurian|Artinskian|||||Overlies Poole Sandstone. Is overlain by Liveringa Group.||
26080|Noonkanbah Formation|62837|5|Briefly described|Stratigraphic columns|||Age: >280-275Ma. Geological Province:  Fitzroy Trough.||||||01-MAR-10
26080|Noonkanbah Formation|64187|5|Briefly described|p320 Fig. 2|Permian|Permian|Underlain by Poole Sandstone, overlain by Liveringa Group. Siltstone, shale, carbonate (marine). Geological Province: Canning Basin.||||||03-FEB-10
26080|Noonkanbah Formation|64580|4|Described|map legend||Early Permian|Siltstone, shale, and sandstone; minor carbonate.||||||09-DEC-08
26080|Noonkanbah Formation|64630|5|Briefly described|p31 Fig.2|Kungurian|Artinskian|Province: Northern and Central Canning Basin.  Underlies the Liveringa Group, overlies the Poole Sandstone. Palynology age: M. trisina to M. villosa.||||||24-NOV-09
26080|Noonkanbah Formation|64643|5|Briefly described|p8, p3 Fig. 2, p5, fig.4, p20|Kungurian|Artinskian|Siltstone-carbonate, up to 650 m thick. Conformably overlies Poole Sandstone.||||||24-NOV-08
26080|Noonkanbah Formation|64971|5|Briefly described|p685 Fig. 2, p689 Fig. 6|Early Permian|Early Permian|||||||09-FEB-10
26080|Noonkanbah Formation|64974|5|Briefly described|p148 Fig. 6, p149|Kungurian|Artinskian|Geological Province: Canning Basin.||||||24-JUN-09
26080|Noonkanbah Formation|64981|5|Briefly described|p669 Fig.3.|Kungurian|Artinskian|||||Overlies Poole Sandstone. Is overlain by Liveringa Formation.|Marine clastic rocks.|
26080|Noonkanbah Formation|64982|6|Mentioned|p700.|Permian|Permian|||||||
26080|Noonkanbah Formation|65301|5|Briefly described|p3, p5 Fig. 4|Middle Permian|Early Permian|Geological province: Canning Basin.||||||
26080|Noonkanbah Formation|65449|5|Briefly described|p5-6|Cisuralian|Cisuralian|Marine sediments.||||Overlies Poole Sandstone. Is overlain by Liveringa Group.||
26080|Noonkanbah Formation|66127|5|Briefly described|Plates 3, 4, 5, 7.|Permian|Permian|||||Overlies Poole Sandstone and is overlain by Liveringa Group.|Well-bedded deltaic to shallow-marine sandstone, siltstone and shale; minor dolomite.|
26080|Noonkanbah Formation|66949|4|Described|p1, p4 Fig.2, p6, p10, p15, p17, p20-23|Artinskian|Artinskian|See also p28, p31, p33, p46-54 Appx.2, p56 Appx. 3, p60-65 Appx.4; p66,68-72,75-89,91 Appx.5; p119-120 Appx.7; Plates 2-10,12. Originally "Noonkanbah Series" of Wade (1937), after Noonkanbah Homestead. Type section detailed and discussed. Up to 640m thick; shallow marine deposits. Contains brachiopods, bryozoans, crinoids and molluscs. May be capable of generating small volumes of gas. Could act as top seal for CO2 sequestration in underlying sandstones. Biostratigraphic zonation. Reservoir and sealing properties discussed. Good to excellent hydrocarbon source potential; minor potential for shale gas. Available core and Formation picks detailed. TOC and Rock-Eval data.||||Conformably overlies Poole Sandstone. Is overlain conformably by Triwhite Sandstone or Lightjack Formation.|Mudstone-dominated, interbedded with sandstone; minor resistant sandy carbonate beds. Includes 4 leucite-bearing lamproite sills.|04-NOV-15
26080|Noonkanbah Formation|67202|5|Briefly described|p44 Fig.2.10, p67-69, p128, p141, p248|Permian|Permian|See also p253, p281. Canning Basin. An aquiclude. Shallow-marine deposits. Very rich marine fauna. Thickness from 6m to 290m. Conductivity image.||Liveringa Group.||Unconformably overlain by the Wallal Sandstone.|Siltstone, poorly bedded and laminated; carbonaceous shale; minor fine-grained sandstone, micaceous, feldspathic.|15-FEB-18
26080|Noonkanbah Formation|67888|6|Mentioned|p42, p82|Triassic|Carboniferous|||||||
26080|Noonkanbah Formation|68007|4|Described|p2, p4, p9, p12, p14-15, Plates 1, 2|Permian|Permian|Canning Basin. 186m thick in Patience 1 and 2 wells. Shallow marine deposits. Potential seal over Permian reservoirs. Composite well log. Early to Middle Permian.||||Overlies Poole Sandstone. Is overlain transitionally by Liveringa Group.|Dominantly interbedded claystone and siltstone, olive-grey to dark grey, commonly slightly pyritic, micaceous and carbonaceous; with minor thin interbeds of light grey, fine- to medium-grained sandstone. Minor pale orange limestone with few fossils.|
26080|Noonkanbah Formation|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Kungurian|Artinskian|Canning Basin. See also 500k_geologyp08_lut.csv.|||||Siltstone, shale, and sandstone; minor carbonate|
26080|Noonkanbah Formation|68902|5|Briefly described|p8, p9 fig 5|Cisuralian|Cisuralian|Not known from boreholes within Waukarlycarly Embayment.||||Overlies Poole Sandstone, overlain by Liveringa Group||
26080|Noonkanbah Formation|69029|5|Briefly described|p319,321,333|Kungurian|Artinskian|Of Canning Basin. Contains the best source rock potential in the Carboniferous-Permian succession in the Canning Basin.||||Overlain by Liverina Group. Underlain by Poole Sandstone.||
26080|Noonkanbah Formation|69099|5|Briefly described|500k_geologyp08_lut.csv|Early Permian|Early Permian||||||siltstone, shale, and sandstone; minor carbonate|
26080|Noonkanbah Formation|69165|4|Described|500k_geologyp08_lut.csv|Permian|Permian||||||Siltstone, Shale and sandstone; minor carbonate.|
26080|Noonkanbah Formation|69182|6|Mentioned|Ch4 p3, Ch4 p9, Ch4 p15-p16|Cisuralian|Cisuralian|Canning Basin. Contains local to regional seals. See also Ch4 p30-p35, Ch4 p38, Ch4 p43, Ch4 p45, Ch4 p47, Ch4 p50-p58, Ch4 p63-p65, Ch4 p74-p77, Ch4 p83-p84, Ch4 p87-p88, Ch4 p90. ||||Conformably overlies the Poole Sandstone. Overlain by the Lightjack Formation.|Shallow marine siltstones and minor carbonate interbeds.|
26080|Noonkanbah Formation|69297|6|Mentioned|p337, p351, p352, p354, p355|Artinskian|Sakmarian|Broome Platform of the Canning Basin. Good sealing rock potential. ||Grant Group||Overlies the Poole Sandstone. Unconformably overlain by the Barbwire Sandstone or the Liveringa Group.||
26080|Noonkanbah Formation|69312|5|Briefly described|p1, p3, p19, p23 fig 27|Permian|Permian|Canning Basin. See also p24 fig 28-29, p26 fig 33, p27, p27 fig 34, p28 fig 35. ||||Overlies the Poole Sandstone. Overlain by the Liveringa Group.|Shale.|
26080|Noonkanbah Formation|69547|5|Briefly described|p182,190,201|Kungurian|Artinskian|Canning Basin. Mud-dominated facies.  Characterised by siliciclastic facies with prominent mud-sand cyclicity in lower part of the section.||||Underlain by Poole Sandstone.||
26080|Noonkanbah Formation|69587|4|Described|GEOL_LUT_CSV files|Kungurian|Artinskian|Of Canning Basin. Events: Alice Springs Orogeny; Point Moody Extension; Prices Creek Movement; Red Bluffs Extension; Van Emmerick Extension. See 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv. |290.1-272.3 Ma (biostrat)||||Siltstone, shale, and sandstone; minor carbonate|
26080|Noonkanbah Formation|69634|5|Briefly described|500k_geologyp08_lut.csv||Early Permian||||||Siltstone, shale, and sandstone; minor carbonate|
26080|Noonkanbah Formation|69693|5|Briefly described|p3|Permian|Permian|Canning Basin. Artinskian to Kungurian. See also reference to Noonkanbah formation (p4).||||Overlies Poole Sandstone. Is overlain by Liveringa Group.||
26080|Noonkanbah Formation|70065|5|Briefly described|Rowley: Fig.2. Regional: Fig.4; p3, p6|Kungurian|Sakmarian|Roebuck Basin.||||Overlies Poole Sandstone. Is overlain by Liveringa Group.|Includes transgressive marine shales.|
26080|Noonkanbah Formation|70129|5|Briefly described|Map legend|Permian|Permian|Canning Basin.|||||Siltstone, shale and sandstone; minor carbonate (section only).|
26080|Noonkanbah Formation|70154|5|Briefly described|500k_interpgeop14_lut.csv|Kungurian|Artinskian||272-290 Ma||||Siltstone, shale, and sandstone; minor carbonate|
26080|Noonkanbah Formation|70762|5|Briefly described|Map legend.|Permian|Permian|Canning Basin.|||||Siltstone, shale and sandstone; minor carbonate.|
26080|Noonkanbah Formation|70774|4|Described|p1-p2, p4-p5, p7-p10|||Canning Basin. Initially defined as the Noonkanbah Series by Wade (1936) and later the Noonkanbah Shale before being renamed the Noonkanbah Formation by Guppy et al., 1951. A type section near Noonkanbah Homestead was proposed by Guppy et al., 1958 before being revised by Mory, 2010. This unit forms the proposed seal over the Grant Group and Poole Sandstone for C02 sequestration. Distribution of facies and wireline characteristics are discussed. Stratigraphic columns are provided in Appendix 2 and lithology is given in detail. See also p18, p25-p26, p31, p34-p35, p37-41, p43, p49, p51-p56, p58-p61, p63, p65, p69, p71-p73, p83-p86, p90-p92, p98-p100, Plate 2, Plate 6.||||Conformably overlies the Poole Sandstone (Grant Group). Conformably overlain by the Liveringa Group.|Siltstone to claystone with local calcareous sandstone and limestone interbedded throughout.|10-FEB-20
26080|Noonkanbah Formation|70826|6|Mentioned|p6 tbl 3|Permian|Permian|Canning Basin.||||||
26080|Noonkanbah Formation|70878|5|Briefly described|p722 Fig.17|Permian|Permian|Fitzroy Trough, NW Canning Basin.||||||
26080|Noonkanbah Formation|71146|5|Briefly described|p6, p12 fig 8,  p43 fig 33|Kungurian|Artinskian|Canning Basin.|||||Mudstone.|
26080|Noonkanbah Formation|71267|4|Described|GEOL_LUT_CSV files|Kungurian|Artinskian|Of Caning Basin. Events: Point Moody Extension (300-242 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 2_5m_interpgeop15_lut.csv.|286-272.3 Ma (biostrat)||||Marine fossiliferous calcareous and micaceous mudstone, siltstone and shale with limestone and fine to medium grained sandstone interbeds and minor granule conglomerate lenses.|
26080|Noonkanbah Formation|71623|5|Briefly described|p344, p345 fig 2|Kungurian|Kungurian|Canning Basin||||Boundary relationships with overlying Lightjack Formation unclear.|Shale|
26080|Noonkanbah Formation|71870|5|Briefly described|p1, p3|Permian|Permian|Canning Basin. A petroleum source interval formed during the Gondwanan supersystem G1.||||Overlies the Poole Sandstone. Overlain by the Liveringa Group.||
26080|Noonkanbah Formation|71892|6|Mentioned|p10|Paleozoic|Paleozoic|||||||
26080|Noonkanbah Formation|71894|5|Briefly described|p4|Cisuralian|Cisuralian|Canning Basin.||||Overlies the Poole Sandstone. Overlain by the Lightjack Formation.|Shale.|
26080|Noonkanbah Formation|72034|5|Briefly described|500k_interpgeop16_lut|Kungurian|Artinskian|Canning Basin.  Age from biostratigraphy.|||||Siltstone, shale, and sandstone; minor carbonate.|
26080|Noonkanbah Formation|72496|6|Mentioned|p220, p223|Kungurian|Artinskian|Canning Basin. Deposited in a shallow marine environment.||||Overlies the Poole Sandstone. Overlain by the Liveringa Group.|Mudstone, minor limestone.|19-MAR-20
26080|Noonkanbah Formation|72497|5|Briefly described|p3 Fig.2, p6 Fig.4, p15|Kungurian|Artinskian|Shown as occurring 5-20km south of the Fitzroy River as part of the St Georges Ranges Anticline north of the underlying Poole Sandstone. Shown as occuring in the Anketell, Tabletop, Ryan Shelves, Willara and Kidson Sub-basins, the Jurgurra and Barbwire Terraces and Broome Platform. Also shown as occuring in the Fitzroy Trough, Betty and Balgo Terraces and part of the Lennard Shelf and Margaret Terrace.||||Conformably overlies Poole Sandstone||
26080|Noonkanbah Formation|72499|4|Described|p1, p5,p6, p7, p8, p10-11, 14, 16.|Guadalupian|Cisuralian|Up to 540m thick. Potential seal for Poole Sandstone, Grant Group. Wide distribution across Canning Basin. Recorded on well logs Sundown 1 and Sundown 3/3H (Lennard Shelf) and The Sisters 1 and Scarpia 1 (Fitzroy Trough),  Frome Rocks 2 (Jurgurra Terrace), Dampier Downs 1, BMR Mount Anderson 1, Roebuck Bay 1. See also p17, p19-20, p22, p24-25, p31, p38, p43-44, p47, p49, p51, p53-54,p57-59,p61, p64-65, p71, p84, p86, p88, p91, p93, p95-96, p98-101.||||Overlies Poole Sandstone and underlies Lightjack Formation. Shown as partially and unconformably underlying Blina Shale.|Dominated by siltstone with minor sandstone/ heterolithic intervals. Includes shale and sandstone-mudstone facies.|
26080|Noonkanbah Formation|72504|6|Mentioned|Figure 2|||Canning Basin. Overlies Poole Sandstone.||||||
26080|Noonkanbah Formation|72505|5|Briefly described|p890, p892-893|Roadian|Sakmarian|Canning Basin. Correlates with the Striatopodocarpites fusus to Dulhuntyispora granulata zones.||||Overlies the Poole Sandstone. Overlain by the Liveringa Group.||
26080|Noonkanbah Formation|73117|5|Briefly described|[See comments].|Kungurian|Asselian|Canning Basin. Contains part of the Pseudoreticulatispora pseudoreticulata Zone [palynology]. p: 3, 14-15, 17, 21, 34, 111, 113, 116-117, 122, 125-127, 131, 116, 135-142.||||Underlain by Poole Sandstone and Clianthus Formation (Grant Group). Unconformably underlain by Luluigui Formation. Overlain by Liveringa Group, including the Lightjack Formation.|Dominantly shale and mudstone with minor sandstone.|
26080|Noonkanbah Formation|73184|6|Mentioned|p187 Fig.3|Kungurian|Artinskian|Canning Basin. Post-glacial.||||Overlies the Poole Sandstone||
26080|Noonkanbah Formation|73445|5|Briefly described|p3, 6, 8, 12-14, 18, 20, 23-24, 28, 34|Permian|Permian|See also p36, 38, 41, 43-46, 50-52, 65-118. Canning Basin. 640m thick. Whole-rock and regolith chemistries tabulated. Multi-element spider diagram.||||Overlies Poole Sandstone. Is overlain by the Liveringa Group and (locally) Callawa Formation..|Siltstone, shale, and less common limestone. Has a high proportion of mudstone relative to sandstone.|
75771|Noonyereena Member|71468|5|Briefly described|p26|||Geological province: Capricorn Orogen, Yilgarn Craton. Of Bryah Sub-basin. Nomenclature by Pirajno et al., 2016 to describe the volcanic components of Karalundi Formation, but has since been made obsolete by subsequent work (see occhipinti et al., 2017) that ascribed the volcanic rocks as intercalated mafic components from the overlying Narracoota Formation due to similar petrological characteristics. A||Unit of Karalundi Formation.||||
75771|Noonyereena Member|71484|5|Briefly described|p126|||Geological province: Of Bryah Basin. Sub-aqueous mafic volcanic rocks interpreted to be part of Karalundi Formation by Pirajno et al. (2015), but are considered to be intercalated volcanic units of the Narracoota Formation instead based on geochemical similarities.||||||30-AUG-19
74802|Norie Group|64891|4|Described|p34 Fig. 1, p37 Fig. 2, p38, p48-9 Tb. 1|Archean|Archean|Basal unit in the newly revised Murchison Supergroup (Van Kranendonk 2008). Includes Murrouli Basalt and Yaloginda Formation. Conformable below Polelle Group. Deposition age: 2820-2800Ma. Geol.prov: Murchison Domain. Basalt, felsic volcaniclastics, BIF||||||07-FEB-11
74802|Norie Group|66195|4|Described|p599 Fig.2, p611 Fig.9, p601, 603, 605|Neoarchean|Mesoarchean||Age ~2825 - 2800 Ma.|Of Murchison Supergroup.||Underlies the Polelle Group, overlies the Golden Grove Group.|Dominated by mafic and ultramafic rocks, also includes locally thick felsic volcanic units as well as banded iron formations and clastic sedimentary rocks.|13-MAR-12
74802|Norie Group|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Unit in Murchison Supergroup.|Includes Murrouli Basalt and Yaloginda Formation.||b|02-MAY-16
74802|Norie Group|67129|4|Described|p17-18, p19 Fig.20, p20, p35, p51, p55|Archean|Archean|Widespread unit. Age range also given as 2820-2805 Ma.|2825-2800 Ma |Murchison Supergroup|Includes Yaloginda Formation, Murrouli Basalt||Mafic-ultramafic volcanics, felsic volcaniclastic sandstones and banded iron formations, intruded at its base by synvolcanic and younger granitic rocks.|07-SEP-17
74802|Norie Group|68107|6|Mentioned|p618, p619 Fig.8|Mesoarchean|Mesoarchean||ca. 2814-2800 Ma|||||
74802|Norie Group|68108|5|Briefly described|p628, p650, p651 Tb.4, p652, p653|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane. U-Pb geochronology by Van Kranendonk & Ivanic (2008).|ca. 2825-2800 Ma||||Felsic volcanics/volcaniclastics, gabbros and dolerite sills.|
74802|Norie Group|68109|5|Briefly described|p659|Neoarchean|Mesoarchean|Murchison Domain.|ca. 2825-2800 Ma|Of the Murchison Supergroup.||Contemporaneous with rocks of the Windimurra and Narndee Igneous Complexes.|Volcanic rocks; contains intervals of BIF.|
74802|Norie Group|68110|3|Fully described|p672-674 Figs.1-3, p675,p678,p681,p691|Neoarchean|Mesoarchean|Murchison Domain. A dolerite sill that intrudes the basalt unit of this group has been dated at 2792 +/- 5 Ma (Van Kranendonk and Ivanic 2009). Geochemistry and geochronology detailed. All samples have undergone crustal contamination.|> 2792 +/- 5 Ma.|Unit in Murchison Supergroup.|Includes Yaloginda Formation and Murrouli Basalt.|Conformably overlain by the Meekatharra Formation (Polelle Group).|Consists of basalt, komatiitic basalt and komatiite with minor felsic volcaniclastic units.|
74802|Norie Group|68287|5|Briefly described|Map Legend|Mesoarchean|Archean||> 2820 Ma|Of the Murchison Supergroup.|Includes Yaloginda Formation.||Psammite; meta banded iron-formation; metarhyolite and banded iron-formation; meta banded chert.|
74802|Norie Group|68519|5|Briefly described|Map Legend|Neoarchean||Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Of the Murchison Supergroup.|Includes Yaloginda Formation.|||
74802|Norie Group|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane. Meta-andesite U-Pb zircon age: 2818 +/-3 Ma as the magmatic crystallization age of the andesite protolith. See geochron file 191056.1.pdf, 193979.1.pdf, 194751.1.pdf for age, relationships.|2820-2805 Ma or 2825-2800 Ma|Murchison Supergroup|Includes Yaloginda Formation, Murrouli Basalt, and 6 unnamed units.|Intruded by Boodanoo Suite.|Andalusite-chlorite(-kyanite-muscovite) schist; quartzite; Metabasalt; basalt; Amphibolite; Felsic volcaniclastic rocks and banded iron-formation; Tremolite--chlorite(--talc) schist.|
74802|Norie Group|68698|5|Briefly described|p2, p4-5, p7, p11, p13, p19, p21|Mesoarchean|Mesoarchean|A major plume event; several kilometres thick.|c.2820-2800 Ma.|Murchison Supergroup.|Murrouli Basalt, Yaloginda Formation|Is overlain by Polelle Group.|Basal komatiites and komatiitic volcaniclastics; then pillowed and massive tholeiitic basalt; rhyolite, felsic volcaniclastic rocks and interbedded shale and/or BIF.|
74802|Norie Group|69014|5|Briefly described|Map Legend||Mesoarchean|Murchison Domain, Youanmi Terrane.||Of the Murchison Supergroup.|Includes the Yaloginda Formation.||Includes volcaniclastics and metamorphosed banded-iron formation; metabasalt and metakomatiitic basalt; foliated metabasalt; felsic schist; meta banded-iron formation; muscovite-rich felsic schist; metamorphosed rhyolite and banded-iron formation.|01-MAY-14
74802|Norie Group|69404|6|Mentioned|p2, p4 Fig.4|Neoarchean|Mesoarchean|Youanmi Terrane. Synchronously deposited with the mafic-ultramafic Narndee and Windimurra Igneous Complexes.|c. 2800 Ma|||||
74802|Norie Group|69583|4|Described|p42, p47, p49, p51-53, p57, p99, p103|Mesoarchean|Mesoarchean|See also p105, p108, p110; Plate 2. Murchison Domain. Several kms thick. Volcanism was accompanied by emplacement of the Annean Supersuite: Meeline Suite and Narndee Igneous Complex. Seismic interpretation.|c.2820-2800 Ma.|Murchison Supergroup.|Murrouli Basalt, Yaloginda Formation.|Is overlain conformably by Polelle Group. Is intruded by Boodanoo Suite (Narndee Igneous Complex). Is sheared against and intruded by Windimurra Igneous Complex.|Basal unit of interbedded Ti-rich, Al-depleted komatiites and komatiitic volcaniclastic rocks, then a thick succession of pillowed and massive tholeiitic basalt, overlain by rhyolite, felsic volcaniclastics, and interbedded BIF and ferruginous shale.|
74802|Norie Group|69584|6|Mentioned|p2, p5 Fig.2, p6, p59, p60, Plate 1|Mesoarchean|Mesoarchean|Subdivided informally in this report into "upper" and "lower" volcanics.|2820 - 2805 Ma (Van Kranendonk et al, 2013)||Murrouli Basalt, Yaloginda Formation|Intruded by the Meeline Suite||
74802|Norie Group|69586|5|Briefly described|p22|Mesoarchean|Mesoarchean|Murchison Domain.||Murchison Supergroup.|Murrouli Basalt, Yaloginda Formation.|Unconformably overlies Minjar Group. Is overlain by Polelle Group.||
74802|Norie Group|69626|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton||Murchison Supergroup|Yaloginda Formation|||
74802|Norie Group|69627|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton||Murchison Supergroup|Yaloginda Formation, Murrouli Basalt|||
74802|Norie Group|69628|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton||Murchison Supergroup|Yaloginda Formation, Murrouli Basalt|||
74802|Norie Group|70020|5|Briefly described|p117-118,128-129|Mesoarchean|Mesoarchean|Geological province: Murchison Domain, Yilgarn Craton. Records a major mantle melting event at c. 2.82 Ga which resulted in the emplacement of large mafic-ultramafic layered intrusions. Associated with VHMS mineralisation.|c. 2825-2805 Ma||Includes Murrouli Basalt Formation and Yaloginda Formation.|Overlain disconformably by Coodardy/Mougooderra Formation/Polelle Group.||
74802|Norie Group|70030|4|Described|p190-192,205|Mesoarchean|Mesoarchean|Geological province: Murchison Domain, Yilgarn Craton. Accompanied by several voluminous mafic intrusive events (e.g. Meeline and Boodanoo suites; Ivanic et al., 2010).|ca. 2825-2805 Ma|Unit of Murchison Supergroup.|Includes Yalogina Formation and Murrouli Basalt.|Overlain by Polelle Group/Coodardy Formation. Underlain by Mount Gibson Group.|Mafic volcanic rocks, felsic volcaniclastic sandstones and banded iron formation.|
74802|Norie Group|70139|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.||Murchison Supergroup.|Murrouli Basalt, Yaloginda Formation.|||
74802|Norie Group|70140|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Murchison Supergroup.|Yaloginda Formation.|||
74802|Norie Group|70226|5|Briefly described|Map legend.|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Carton. 17 facies are mapped separately.|2825-2800 Ma||||Conglomerate, sandstone, arkose, siltstone, shale, pelite, chert, banded iron formation; basalt; volcaniclastic (rhyolitic to dacitic) sandstone to siltstone; schist (psammitic or mafic volcanic); amphibolite; sheared, metamorphosed, deeply weathered|16-DEC-15
74802|Norie Group|70332|6|Mentioned|p77, 79, 81|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Sourced by the Norie mantle plume (Wyman and Kerrich, 2012).|2820-2805 Ma.|Murchison Supergroup.|||Basaltic magmatism; greenstones.|
74802|Norie Group|70418|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|2825-2800 Ma.|Murchison Supergroup.|Murrouli Basalt, Yaloginda Formation.|||
74802|Norie Group|70419|5|Briefly described|p1-3, p9, p12, p15, p17, p26 Fig.10|Mesoarchean|Mesoarchean|A dominant greenstone supracrustal unit. Density is 2.66 g/cm3.|2819 Ma.|Murchison Supergroup.|Yaloginda Formation.|Is intruded by Windimurra Igneous Complex.|Metasedimentary rocks; includes psammitic schist.|
74802|Norie Group|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton. The three facies are mapped separately.|2825-2800 Ma.|Murchison Supergroup.|||Mafic schist after volcanic rock; metamorphosed BIF locally with recrystallised quartz and magnetite, moderately deformed; metamorphosed, moderately well-bedded volcaniclastic sandstone to siltstone of rhyolitic to dacitic affinity.|
74802|Norie Group|70770|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Murchison Supergroup.|Yaloginda Formation.||Metamorphosed BIF, chert, siliciclastic, volcanic and volcaniclastic rocks. Also includes amphibolite and local metabasalt; fine- to medium-grained; typically foliated and lineated.|
74802|Norie Group|70796|4|Described|2_5m_interpgeop15_lut.csv|Mesoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. Affected by the Yilgarn Craton granite magmatism (3010  2600 Ma); Youanmi Terrane events (3131  2600 Ma). See also 100k_geologyl_lut.csv, 100k_geologyp_lut.csv, 100k_geologysub_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 178142.1.pdf, 183953.1.pdf, 185920.1.pdf, 185958.1.pdf, 185998.1.pdf, 191056.1.pdf, 193979.1.pdf, 194751.1.pdf, 198209.1.pdf, 198210.1.pdf, 198228.1.pdf, 198293.1.pdf, 198295.1.pdf, 198298.1.pdf211101.1.pdf, Austin100_2442_stratig.pdf, Badja100_2240_stratig.pdf, Bungar100_2539_stratig.pdf, Challa100_2541_stratig.pdf, Coolamaninu100_2540_stratig.pdf, Cue100_2443_stratig.pdf, MountMagnet100_2441_stratig.pdf, Reedy100_2543_stratig.pdf, Windimurra100_2641_stratig.pdf, Wynyangoo100_2542_stratig.pdf, Yalgoo100_2241_stratig.pdf, Youanmi100_2640_stratig.pdf. Numerous additional lithologies are provided. Isotopically dated at 2813 +/ 3 Ma.|ca 2825 to 2800 Ma (inferred)|Murchison Supergroup|Includes the Yaloginda Formation and the Murrouli Basalt.|Intruded by the Annean Supersuite and the Boodanoo Suite. Unconformably overlain by the Mougooderra Formation.|Metabasalt, felsic volcaniclastic rocks, and banded ironformation; strongly to weakly metamorphosed. Quartzite, metamorphosed bandediron formation, psammite, metasandstone, local metaconglomerate and metachert, ultramafic schist.|
74802|Norie Group|70826|6|Mentioned|p6 tbl 2, p8|Neoarchean|Neoarchean|Youanmi Terrane.||Murchison Supergroup||||22-APR-20
74802|Norie Group|70830|4|Described|p3, p5, p7-p9, p12, p14, p27-p28, p58|Neoarchean|Mesoarchean||c. 2825-2800 Ma|Murchison Supergroup|Includes the Murrouli Basalt and the Yaloginda Formation.|Conformably overlain by the Polelle Group. Intruded by the Narndee Igneous Complex and Meeline Suite.||
74802|Norie Group|71148|6|Mentioned|p120|Neoarchean|Neoarchean|Cue Zone, northern Youanmi Terrane, Yilgarn Craton. Plume-related. Associated with VHMS mineralisation.|c.2815 Ma (eruption).|||||
74802|Norie Group|71159|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.||Murchison Supergroup.|Yaloginda Formation.|||
74802|Norie Group|71168|4|Described|iii, p7-p8, p10, |Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Exposed across the northern parts of the Murchison Domain and records a major mantle melting event at 2.82 Ga which resulted in the emplacement of large mafic-ultramafic layered intrusions. See also p18-p19, p21-p22, p40 fig 25, p51, p56.|c. 2825-2805 Ma||Includes the Yaloginda Formation and the Murrouli Basalt.|Overlies the Narndee Igneous Complex. Overlain by the Polelle Group.||
74802|Norie Group|71269|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). Strongly folded, and is metamorphosed to upper greenschist or amphibolite facies. Sample GSWA 193979 (fine-grained meta-andesite) yielded a weighted mean 207Pb/206Pb date of 2818+\-3 Ma, interpreted as the magmatic crystallization age of the andesite protolith. Sample GSWA 198228 (altered volcaniclastic metasandstone) yielded a weighted mean 207Pb/206Pb date of 2805+\-5 Ma, interpreted as the maximum depositional age for the sandstone protolith. Sample GSWA 198293 (altered volcaniclastic metasandstone) yielded a weighted mean 207Pb/206Pb date of 2826+\-7 Ma, interpreted as the maximum depositional age for the sandstone protolith.  Sample GSWA 198298 (metadacite) yielded a weighted mean 207Pb/206Pb date of 2813+\-3 Ma, interpreted as the magmatic crystallization age of the dacite. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv, 100k_geologysub_lut.csv.|2825-2800 Ma; 2813+\-3 Ma|Unit of Murchison Supergroup.|Includes Murrouli Basalt, Yaloginda Formation.|In contact with Bunnawarra Suite plutons. Intruded by Boodanoo Suite and Meeline Suite.|Basalt; amygaloidal, pillow, komatiitic, pyroxene spinefix; metabasalt: interlayered with psammitic sedimentary rocks; schist; mafic, tremolite-rich ultramafic, andalusite-chlorite-kyanite-muscovite; metamorphosed cherts and BIFs, quartzite.|
74802|Norie Group|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.||Murchison Supergroup.|Murrouli Basalt, Yaloginda Formation.|||
74802|Norie Group|71272|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. The three facies are mapped separately.|2825-2800 Ma.|Murchison Supergroup.|||Metabasalt, felsic volcaniclastic rocks, and BIF; strongly to weakly metamorphosed. Quartzite, commonly foliated, local relict bedding. Metamorphosed BIF locally with recrystallised quartz and magnetite, typically moderately deformed.|
74802|Norie Group|71809|5|Briefly described|map legend|Mesoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane|~2825-2800 Ma.|Of Murchison Supergroup.|Includes Singleton Formation.|||06-SEP-19
74802|Norie Group|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Youanmi Terrane. |||Includes Yaloginda Formation, Murrouli Basalt and 3 unnamed units.||Andalusite-chlorite(-kyanite-muscovite) schist; porphyroblastic; strongly foliated/lineated. Tremolite-rich ultramafic schist; locally interlayered with basalt, metadolerite, or mafic schist; typically sheared. Basaltic volcanic rock; metamorphosed.|
74802|Norie Group|72389|5|Briefly described|Map Legend|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Gabanintha 1:100k map sheet 2644.|2825-2800 Ma|Murchison Supergroup|Includes the Yaloginda Formation and the Singleton Formation.|||28-AUG-20
74802|Norie Group|72494|5|Briefly described|p15, p17 Fig.3, p18, 21, 28-31|||Murchison Domain, Youanmi Terrane, Yilgarn Craton. Tectonics of source melts discussed. Volcanism was related to subduction, not mantle plume incubation.|<2799 +/- 2 Ma.||Singleton Formation.|Is overlain conformably by the Meekatharra Formation (Polelle Group).|Pyroxene spinifex basalt with interlayered schist; mafic schist, local pyroxene spinifex; BIF.|
74802|Norie Group|73023|5|Briefly described|p2-3|Mesoarchaean|Mesoarchaean||2820-2800 Ma.|||Unconformably overlies Gossan Hill Formation. Is overlain unconformably by Mougooderra Formation.|Greenstone sequences.|
74802|Norie Group|73410|5|Briefly described|p13||||c.2825-2800 Ma.||Yaloginda Formation.||Ultramafic and mafic schists, BIF.|
74802|Norie Group|73453|5|Briefly described|p3|Mesoarchean|Mesoarchean|Youanmi Terrane (Murchison).|2825-2800 Ma||||Mafic and felsic volcanics.|
74802|Norie Group|73596|5|Briefly described|p1161, 1163, 1169-1170, 1172|Mesoarchean|Mesoarchean|Youanmi Terrane.|2825-2800 Ma.|Murchison Supergroup.|Yaloginda Formation; Lower Marda Formation; Lady Alma Igneous Complex.|Overlies Golden Grove Group. Is overlain unconformably by Polelle or Glen Group.|Mafic and ultramafic volcanic rocks interlayered with BIF. Contains boninite-like rocks and high-Mg andesites.|
38518|Norseman Formation|23488|5|Briefly described|p40|||Calcareous unit - probably equivalent to the Paling Member of Wilson Bluff Limestone.  Geological Province: Bremer Basin.||||||05-JUL-05
38518|Norseman Formation|24397|4|Described|p239|Middle Eocene|Middle Eocene|Originally defined as Norseman Limestone. Overlies North Royal Formation. Geological Province: Eucla Basin.||||||31-AUG-09
38518|Norseman Formation|61814|5|Briefly described|p22|Middle Eocene|Middle Eocene|Fossiliferous marine carbonate, shallow water deposit.||||||08-FEB-10
38518|Norseman Formation|64340|5|Briefly described|p26 Tb. 5, p28|Middle Eocene|Middle Eocene|Of Eundyine Group. Underlain by North Royal Formation. Fossiliferous limestone.||||||12-SEP-13
38518|Norseman Formation|64646|6|Mentioned|p23 Fig. 3, p24 Fig. 4|Late Eocene|Middle Eocene|Geological Province: Yilgarn Craton.||||||08-FEB-10
38518|Norseman Formation|65194|5|Briefly described|p138 Fig.4.38|Middle Eocene|Middle Eocene|Probably supersedes Norseman Limestone. Used 2003, 2008. Appears to be entirely enclosed by Werrillup Formation.||||||
38518|Norseman Formation|65260|6|Mentioned|p27 Fig.20|Upper Eocene|Middle Eocene|Of Eundynie Group in Cowan Palaeovalley. Also referred to as Norseman Limestone on the same page.||||||
38518|Norseman Formation|69598|5|Briefly described|p2, p9, p10, p11, p11 Tb.1, p29 Tb.4|Middle Eocene|Middle Eocene|Eucla Basin. Up to 45m thick. Potential carbon dioxide storage reservoir.||Eundynie Group|||Calcareous, fossiliferous sandstone and interbedded grainstone that is overlain by grainstone to rudstone succession.|
36956|North Pole Monzogranite|23416|5|Briefly described|Map Legend|Archean|Archean|In the Pilbara Craton.||||||07-NOV-08
36956|North Pole Monzogranite|23755|4|Described|p29|Archean|Archean|Age: 3459+/-18 Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
36956|North Pole Monzogranite|23783|5|Briefly described|p53|Archean|Archean|Age: 3459+/-18Ma.  See also p65.||||||07-NOV-08
36956|North Pole Monzogranite|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Age: 3459+/-18Ma (Thorpe et al, 1992a).  Geological Province: Pilbara Craton.||||||07-NOV-08
36956|North Pole Monzogranite|24110|5|Briefly described|Plate 1|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
36956|North Pole Monzogranite|24184|5|Briefly described|p701|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
36956|North Pole Monzogranite|60112|5|Briefly described|p105, p107-117. |||A volumetrically insignificant intrusive granite body; a shallow, steeply plunging plug overlying greenstones and formed by fold interference, not diapirism. U-Pb whole zircon age.|3459 +/- 18 Ma (Thorpe et al., 1992)|Unit in Warrawoona Group.||Comagmatic with the Panorama Formation|Consists of medium- to coarse-grained, massive to weakly foliated, and homogeneous biotite monzogranite.|
36956|North Pole Monzogranite|61111|5|Briefly described|p98||Paleoarchean||c.3458 Ma.|||||
36956|North Pole Monzogranite|61252|6|Mentioned|p65, p67|Archean|Archean|Same as North Pole Adamellite? Age: c.3459 Ma.||||||07-NOV-08
36956|North Pole Monzogranite|61253|5|Briefly described|p56|Archean|Archean|Sub-volcanic intrusion.  Age: 3.46Ga.  Geological Province: Pilbara Craton.||||||07-NOV-08
36956|North Pole Monzogranite|61257|5|Briefly described|p353|Archean|Archean|Geological Province: North Pole Dome of the Pilbara Craton.||||||07-NOV-08
36956|North Pole Monzogranite|62979|5|Briefly described|p211, p213|||Intrusive rocks in the core of the North Pole Dome. Geological Province: Pilbara Craton.||||||07-FEB-11
36956|North Pole Monzogranite|63441|5|Briefly described|p7 Tb. 2|Archean|Archean|Supersedes North Pole Adamellite. Geological province: Pilbara Craton.||||||07-FEB-11
36956|North Pole Monzogranite|64580|4|Described|map legend||Paleoarchean|Of Callina Supersuite. Biotite monzogranite; equigranular to weakly porphyritic.||||||15-DEC-08
36956|North Pole Monzogranite|64747|5|Briefly described|p95-96|Paleoarchean|Paleoarchean|Emplaced into a dome as a subvolcanic laccolith while Panorama Formation was erupting.|3459 +/- 18 Ma (U-Pb zircon).|||Intruded beneath Panorama Formation.||
36956|North Pole Monzogranite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Callina Supersuite. Aged c.3459 Ma. Biotite monzogranite; equigranular to weakly porphyritic.||||||
36956|North Pole Monzogranite|67130|6|Mentioned|p62|Paleoarchean|Paleoarchean|Amphibolite facies contact aureole developed around this unit.|3459 +/- 18 Ma|||||
36956|North Pole Monzogranite|67197|6|Mentioned|p6|||||||||
36956|North Pole Monzogranite|67269|5|Briefly described|p5-6, p8-9, p12|Paleoarchean|Paleoarchean|||||Intrudes North Star Basalt.|Biotite monzogranite.|
36956|North Pole Monzogranite|68280|6|Mentioned|p1, p2|Paleoarchean|Paleoarchean||3459 +/- 18 Ma|||||
36956|North Pole Monzogranite|68312|6|Mentioned|p103|Archean|Archean|North Pole Dome, Pilbara Craton.||||||
36956|North Pole Monzogranite|69015|5|Briefly described|Map Legend||Paleoarchean|East Pilbara Terrane, Pilbara Craton.|< 3459 Ma (Thorpe et al. 2002)|Of the Tambina Supersuite.|||Biotite monzogranite; equigranular to weakly porphyritic.|01-MAY-14
36956|North Pole Monzogranite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Tambina Supersuite|||Biotite monzogranite; equigranular to weakly porphyritic|
36956|North Pole Monzogranite|69185|4|Described|GEOL_LUT_CSV files||Paleoarchean|Geological province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 3459 Ma|Unit of Callina Supersuite.|||Biotite monzogranite; equigranular to weakly porphyritic|
36956|North Pole Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|3459-3430 Ma (isotopic, inferred)|Unit of Tambina Supersuite.|||Biotite monzogranite; equigranular to weakly porphyritic|
36956|North Pole Monzogranite|70507|6|Mentioned|p430-431|Archean|Archean|Geological province: Pilbara Craton. Emplaced within the North Pole Dome at ~3.46 Ga (Van Kranendonk et al., 2008).|~3.46 Ga|||||
36956|North Pole Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
36956|North Pole Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|||Tambina Supersuite|||Biotite monzogranite; equigranular to weakly porphyritic.|
36956|North Pole Monzogranite|72251|6|Mentioned|p55|||Of Shaw Granitic Complex. Intrudes a greenstone belt 20km N of Shaw Granitic Complex. Coeval with North Shaw Suite. U-Pb zircon age of 3.459+\-0.018 Ga (Thorpe et al., 1992).||||||
36956|North Pole Monzogranite|73160|5|Briefly described|p2 Fig.1, p3-4, p6|Paleoarchean|Paleoarchean|Pilbara Craton, East Pilbara Terrane. Forms the core of the North Pole Dome, acted as the subvolcanic feeder to felsic volcanic rocks of the Panorama Formation.|3454 +/- 17 Ma|||Intrudes North Star Basalt.||
27215|North Rankin Formation|6876|6|Mentioned|p100 Fig.5.|Early Jurassic|Early Jurassic|||||||
27215|North Rankin Formation|12498|5|Briefly described|p517 Fig.3. |Early Jurassic|Early Jurassic|Lambert 2 drilling in 1996 intersected a gross 133 m gas column. Marginal to shallow-marine deposits with two main reservoir facies.||||Overlies Brigadier Formation. Is overlain by Murat Siltstone.|Interbedded sandstones and shales, generally coarsening-up, and clean blocky 20 to 30 m thick sandstones with sharp boundaries and poorly defined fining-upwards character.|
27215|North Rankin Formation|23726|5|Briefly described|p8 Fig 2c|Early Jurassic|Early Jurassic|Overlying unit Legendre Formation. Underlying unit Brigadier Formation. Geological Province: Carnarvon Basin.||||||
27215|North Rankin Formation|24246|6|Mentioned|p19|||Geological Province: Carnarvon Basin.||||||
27215|North Rankin Formation|24390|5|Briefly described|p24 Table 6|||Geological Province: Northern Carnarvon Basin.||||||
27215|North Rankin Formation|40617|2|Defined|p7|Early Jurassic|Early Jurassic|Late Triassic to Early Jurassic.||||||01-SEP-08
27215|North Rankin Formation|40992|6|Mentioned|Fig.8|||||||||
27215|North Rankin Formation|41271|3|Fully described|p116|||||||||
27215|North Rankin Formation|41440|6|Mentioned|p136|||||||||
27215|North Rankin Formation|41732|6|Mentioned|p534|||||||||
27215|North Rankin Formation|41751|6|Mentioned|p4|||||||||
27215|North Rankin Formation|42116|5|Briefly described|Fig.1 P6|||||||||
27215|North Rankin Formation|42615|3|Fully described|P 28|Sinemurian||Variation on North Rankin Beds. Age: Early Jurassic (late Sinemurian).||||||01-SEP-08
27215|North Rankin Formation|50085|5|Briefly described|p24 Tb. 6|Early Jurassic|Early Jurassic|Geological Province: Northern Carnarvon Basin (Barrow Sub-basin).||||||
27215|North Rankin Formation|62734|5|Briefly described|p1362 Fig. 2|Early Jurassic|Early Jurassic|Geological Province: Barrow Sub-basin.||||||01-SEP-08
27215|North Rankin Formation|62837|5|Briefly described|Stratigraphic columns|Early Jurassic|Early Jurassic|Age: ~203-~190Ma. Geological Province: Dampier Sub-basin, Rankin Platform and Beagle Sub-basin.||||||07-NOV-06
27215|North Rankin Formation|63936|4|Described|p181, p185|||Originally North Rankin Beds (Crostella and Barter, 1980). Formalised as North Rankin Formation by Hocking (1985). The type section is the interval 3074-3185m in North Rankin 3 (depths revised by Hocking, 1992), entirely within the C. torosa Spore-pollen zone. Northern Carnarvon Basin. Palynofacies and palynological zones detailed. Marginal marine deposits.|||Unconformably overlies Brigadier Formation.||Dominantly sandstone.|
27215|North Rankin Formation|63950|5|Briefly described|p336 Fig. 4|Early Jurassic|Early Jurassic|Overlies Brigadier Formation; underlies Murat Siltstone. Geological Province: northern Carnarvon Basin.||||||27-MAY-08
27215|North Rankin Formation|64978|6|Mentioned|p528 Fig.2.|Early Jurassic|Early Jurassic|||||||
27215|North Rankin Formation|64979|6|Mentioned|p547 Fig.14|||||||||
27215|North Rankin Formation|67200|5|Briefly described|p8 fig 6, |Jurassic|Jurassic|||||Overlies Brigadier Formation, overlain by Legendre Formation|Sandstone and siltstone.|
27215|North Rankin Formation|67369|6|Mentioned|p246 Fig.3. |Sinemurian|Hettangian|Dampier Sub-basin.||||Overlies Brigadier Formation.||
27215|North Rankin Formation|68135|5|Briefly described|p51 fig 2a|Hettangian|Hettangian|Northern Carnarvon Basin.||||Overlies Brigadier Formation. Is overlain by Murat Siltstone.||14-SEP-17
27215|North Rankin Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Northern Carnarvon Basin.||||Overlies Brigadier Formation. Is overlain by Athol, Legendre Formations.||
27215|North Rankin Formation|70066|5|Briefly described|Dampier: Fig.2; p2-3. Exmouth: Fig.2|Sinemurian|Hettangian|See also Regional: Fig.6; p4. Seggie et al. (2007). Northern Carnarvon Basin. Fluvio-deltaic to marine sediments are potential reservoirs on Rankin Platform.||||Overlies Brigadier Formation. Is overlain by Murat Siltstone.|Thin, reservoir-quality sandstones preserved on some horst blocks.|
27215|North Rankin Formation|70906|5|Briefly described|p757|Jurassic|Jurassic|Gorgon Platform.||||Overlies Mungaroo Formation. Is overlain by Murat Siltstone.||
27215|North Rankin Formation|73564|5|Briefly described|p1223, 1225|Jurassic|Jurassic|Exmouth Plateau, Gascoyne Margin.||||Overlies Brigadier Formation. Is overlain by Murat Siltstone.|Shallow- to deep-marine clastic sediments.|
73782|North Ravensthorpe pegmatites|50542|5|Briefly described|p123-124|||Informal name. Gently dipping. Thickness: 21m. Geological Province:Yilgarn Craton.||||||07-FEB-11
37213|North Royal Formation|24397|3|Fully described|p235|Middle Eocene|Middle Eocene|Equivalent to Maralinga Formation in South Australia. Consists of sediments formerly included in lower Werrillup and lower Pidinga Fms. and Wollubar Sst.  Not related to Princess Royal Fm.  Overlain by Norseman Fm.  Geological Province: Eucla Basin.||||||
37213|North Royal Formation|64340|5|Briefly described|p26 Tb. 5, p28, p31|Middle Eocene|Middle Eocene|Of Eundynie Group. Overlain by Norseman Formation. Non-marine to marginal-marine, fluviodeltaic to estuarine sediments.||||||16-MAY-14
37213|North Royal Formation|65194|5|Briefly described|p138 Fig.4.38|Middle Eocene|Middle Eocene|?Of Clarke et al (2003), who seem to have this unit supersede Pidinga Formation in Lefroy Palaeovalley, and the lower part of Werrillup Formation in Cowan Palaeovalley. Hou et al (2008) appear to regard this unit as obsolete, replaced by Werrillup Formation.||||||
37213|North Royal Formation|65260|6|Mentioned|p26-27, p27 Fig.20|Middle Eocene|Middle Eocene|Non-marine to marginal marine quartz sands, clay and lignite; overlain by Werrillup Formation. Proposed name (by Clarke 2003) includes Lower Werrillup Formation in Eundynie Group. ||||||
37213|North Royal Formation|69598|5|Briefly described|p2, p9, p10, p11 Tb.1, p29 Tb.4|Middle Eocene|Middle Eocene|Eucla Basin. Up to 50m thick. Potential carbon dioxide storage reservoir; also contains potential sealing lithologies. Formerly the Lower Werrilup Formation. Deposited in a non-marine to marginal marine environment.  |||||Lignitic claystones and siltstones.|
34106|North Shaw Suite|22615|5|Briefly described|p 8||Archean|Age: 3460Ma.||||||07-NOV-08
34106|North Shaw Suite|23755|5|Briefly described|p9|||Informal? Same as Shaw Granitoid Complex. Of the North Shaw Granitoid Complex. Age: 3499+/-22 Ma.||||||
34106|North Shaw Suite|23783|5|Briefly described|p19|Archean|Archean|||||||07-NOV-08
34106|North Shaw Suite|23895|5|Briefly described|p886, 887 Fig.3|||Part of Shaw Granitoid Complex.||||||
34106|North Shaw Suite|24531|5|Briefly described|p6, p27|Archean|Archean|Northern part of the Shaw Granitoid Complex.  Age: 3499-3450Ma.||||||07-NOV-08
34106|North Shaw Suite|44150|5|Briefly described|p143 Tb.2-21, p155 Fig.2-142|||Of Bickle et al.(1983, 1985). Yule Granitoid Complex|||Includes North Shaw Tonalite.|||
34106|North Shaw Suite|50423|4|Described|p217||Archean|Age: 3470 Ma. Tonalites, granodiorites and diorites emplaced as semi-concordant sheets at ~5km depth. Intrudes greenstones. Of Shaw Granitoid Complex.||||||07-NOV-08
34106|North Shaw Suite|50427|5|Briefly described|p186|Archean|Archean|Of Shaw Granitoid Complex.||||||07-NOV-08
34106|North Shaw Suite|63441|5|Briefly described|p35, p7 Tb. 2|Archean|Archean|Contains Coolyia Creek Granodiorite and North Shaw Tonalite with ages 3469+/-2Ma and 3468+/-5Ma respectively. Geological province: Pilbara Craton.||||||07-FEB-11
34106|North Shaw Suite|66217|5|Briefly described|p8, p24. |Paleoarchean|Paleoarchean|Of Bickle et al 1983. Calc-alkaline. Well-preserved.|c.3467 Ma.|Unit in Callina Supersuite, Shaw Granitic Complex.||||10-JUN-20
34106|North Shaw Suite|69167|6|Mentioned|142962.1.pdf|Archaean|Archaean||||Includes Coolyia Creek Tonalite|||
34106|North Shaw Suite|69590|5|Briefly described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Samples GSWA 142878 (foliated biotite monzogranite) occurs as a sheeted sill complex and yielded an interpreted crystallisation age of 3445+\-3 Ma (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.||Unit of Callina Supersuite.|Includes Coolyia Creek Granodiorite, North Shaw Tonalite.|||
34106|North Shaw Suite|72251|6|Mentioned|p55|||Of Shaw Granitic Complex. Coeval with North Pole Monzogranite.||||||
34106|North Shaw Suite|72668|6|Mentioned|p9, p24|||Has compositions consistent with the Archean TTG series.|c. 3460 Ma|Of Callina Supersuite.|||Includes TTG granites.|
24433|North Shaw Tonalite|23416|5|Briefly described|Map Legend|Archean|Archean|Of Shaw Granitoid Complex, Pilbara Craton||||||07-NOV-08
24433|North Shaw Tonalite|23755|4|Described|p48|Archean|Archean|Age: >3480 Ma. See also page 18 Table 2. Of North Shaw Suite.||||||07-NOV-08
24433|North Shaw Tonalite|24531|5|Briefly described|p26|Archean|Archean|Age: 3436+/-2Ma (Zegers, 1996).||||||07-NOV-08
24433|North Shaw Tonalite|38542|6|Mentioned|p362|||||||||
24433|North Shaw Tonalite|39444|2|Defined|Table 3|Archean|Archean|See also Table 2.||||||07-NOV-08
24433|North Shaw Tonalite|39697|3|Fully described|p35|||||||||
24433|North Shaw Tonalite|44150|5|Briefly described|p143 Tb.2-21, p148 Fig.2-136|||Shaw Granitoid Complex||North Shaw Suite.|||Biotite tonalite, minor biotite and hornblende granodiorite, weakly foliated.|
24433|North Shaw Tonalite|50381|5|Briefly described|Map Legend|Archean|Archean|Of Shaw Granitoid Complex. Geological Province: Pilbara Craton. Age: c. 3493-3470 Ma||||||07-NOV-08
24433|North Shaw Tonalite|50423|5|Briefly described|p215, Fig.1||Archean|Age: c. 3490 Ma. Of North Shaw Suite.||||||07-NOV-08
24433|North Shaw Tonalite|50427|5|Briefly described|p186|Archean|Archean|Age: 3500-3451 Ma. Of Shaw Granitoid Complex.||||||07-NOV-08
24433|North Shaw Tonalite|63441|5|Briefly described|p7 Tb. 2|Archean|Archean|Of the North Shaw Suite. Age: 3468+/-5Ma. Geological province: Pilbara Craton.||||||07-FEB-11
24433|North Shaw Tonalite|63538|6|Mentioned|p22|||||||||07-FEB-11
24433|North Shaw Tonalite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Callina Supersuite. Aged c.3468 Ma. Meta hornblende tonalite to diorite; equigranular, with local plagioclase phenocrysts.||||||
24433|North Shaw Tonalite|69012|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane.|c. 3468 Ma|Of the Callina Supersuite.|||Comprises meta hornblende tonalite to diorite; equigranular, with local plagioclase phenocrysts.|
24433|North Shaw Tonalite|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. |c. 3468 Ma||||Meta hornblende tonalite to diorite; equigranular, with local plagioclase phenocrysts.|01-MAY-14
24433|North Shaw Tonalite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Age derived from sample of hornblende-biotite-quartz monzodiorite (178044.1.pdf)|3468 +/- 5 Ma (SHRIMP)|Callina Supersuite|||Meta hornblende tonalite to diorite; equigranular, with local plagioclase phenocrysts|
24433|North Shaw Tonalite|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA 178044 (hbl-bt qtz monzodiorite) yielded an interpreted igneous crystallisation age of 3468+\-5 Ma for teh monzodiorite (weighed mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|3468-3466 Ma (Isotopic)|Unit of North Shaw Suite.|||Metamorphosed hornblende tonalite to diorite; equigranular, with local plagioclase phenocrysts|
24433|North Shaw Tonalite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||diorite, tonalite|
24433|North Shaw Tonalite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||3468+/-2 Ma.|Callina Supersuite|||Metamorphosed hornblende tonalite to diorite; equigranular, with local plagioclase phenocrysts.|
31686|North Whundo Intrusion|24353|6|Mentioned|p9 Fig.5|Archean|Archean|Intrudes the Tozer Formation (Whundo Group). Overlain by Yannery Granite. Geological Province: Pilbara Craton||||||07-NOV-08
31686|North Whundo Intrusion|43822|5|Briefly described|map legend|Archean|Archean|Layered mafic intrusions approx. 2925 Ma. Of Pilbara Supergroup.||||||07-NOV-08
31686|North Whundo Intrusion|63441|5|Briefly described|p12 Tb. 2, p38|Archean|Archean|Of the Radley Suite. Contains rocks of the former Yannery Granite. Age: 2930+/-4Ma. Mafic layered intrusion. Geological Province: West Pilbara Superterrane.||||||07-FEB-11
31686|North Whundo Intrusion|64174|5|Briefly described|Map legend|Archean|Archean|Part of the Radley Suite (Sisters Supersuite). Gabbro, pyroxenite, and dolerite; metamorphosed.||||||07-NOV-08
31686|North Whundo Intrusion|64580|4|Described|map legend||Mesoarchean|Of Radley Suite. Gabbro, leucogabbro, and dolerite; metamorphosed.||||||15-DEC-08
31686|North Whundo Intrusion|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Radley Suite.|||Gabbro, leucogabbro, and dolerite; metamorphosed|
31686|North Whundo Intrusion|70775|6|Mentioned|p66|||||Radley Suite||||
31686|North Whundo Intrusion|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||gabbro, dolerite, anorthosite|
31686|North Whundo Intrusion|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Radley Suite|||Gabbro, leucogabbro, and dolerite; metamorphosed.|
31132|Norton Metagabbro|43484|6|Mentioned|11|||||||||
31132|Norton Metagabbro|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Tickalara Metamorphics.|||Metamorphosed gabbro: clinopyroxene-orthopyroxene-magnetite-plagioclase-quartz(-hornblende-biotite) mafic granulite|
69694|Nullagine Group|61253|4|Described|p56, p53 Fig. 2|Archean|Archean|Of the De Grey Supergroup.  Comprises Mosquito Creek and Coondamar Formations. Unconformable on Kelly Group and on Copper Gorge Formation.  Age: 2.95-2.92Ga.  Geological Province: eastern Pilbara Craton - Mosquito Creek Basin.||||||07-NOV-08
69694|Nullagine Group|61264|5|Briefly described|p64 Fig. 2|Archean|Archean|Of the De Grey Supergroup. Includes Mosquito Creek and Coondamar Formations. Geological Province: Mosquito Creek Basin/Pilbara Craton.||||||07-NOV-08
69694|Nullagine Group|63417|5|Briefly described|Map legend|Archean|Archean|Of De Grey Supergroup.  Includes Coondamar and Mosquito Creek Formations. Min. age: <2950Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
69694|Nullagine Group|63441|5|Briefly described|p2, p29|Archean|Archean|The term "Nullagine" was formerly used as Series or Beds to refer to rocks of the Fortescue Group; it is now used to refer to basin fill in Mosquito Creek Basin and comprises Coondamar and Mosquito Creek Formations. Of De Grey Supergroup. Age: 2970-2930Ma||||||07-FEB-11
69694|Nullagine Group|63538|5|Briefly described|p2 Fig. 1, p6 Fig. 3|Archaean|Archaean|Of De Grey Supergroup. Age: 2970-2930 Ma. Geological Province: De Grey Superbasin.||||||19-APR-13
69694|Nullagine Group|63854|5|Briefly described|p229 Fig.2|||||Of the DeGrey Supergroup.|Includes the Mosquito Creek and Coondamar Formations|||
69694|Nullagine Group|64580|4|Described|map legend|Mesoarchean|Paleoarchean|Psammite and pelite, interbedded.||||||15-DEC-08
69694|Nullagine Group|64632|6|Mentioned|p201 Fig.1|Mesoarchean|Mesoarchean||2970-2930 Ma |Of the De Grey Supergroup.||||
69694|Nullagine Group|64654|5|Briefly described|Map Legend|Archaean|Archaean|Of De Grey Supergroup. Geological Province: Pilbara Craton.||||||17-NOV-08
69694|Nullagine Group|64656|5|Briefly described|Map Legend|Archaean|Archaean|Of Pilbara Supergroup. Includes Coondamar and Mosquito Creek Formations. Geological Province: Pilbara Craton.||||||26-NOV-08
69694|Nullagine Group|65825|6|Mentioned|pp31-32.|||Appendix 2 shows this as including the Mosquito Creek and Coondamar Formations, and as a unit of the De Grey Supergroup, according to the GSWA databases.|||Includes Mosquito Creek Formation.|||
69694|Nullagine Group|66118|4|Described|p146 Fig.1, p147|||Pilbara Craton.|2970-2930 Ma|De Grey Supergroup||Unconformably overlies Whim Creek Group.||
69694|Nullagine Group|66217|5|Briefly described|p39, p40.|Mesoarchean|Mesoarchean|Mosquito Creek Basin, Pilbara Craton. Deformed during north-south compression at 2930-2905 Ma. Hosts shear-zone hosted, epigenetic and epithermal gold deposits.|>2926 Ma.|Unit in De Grey Supergroup.|||Dominantly coarse- to fine-grained clastic sedimentary rocks (turbidites).|
69694|Nullagine Group|67130|6|Mentioned|p13|||||De Grey Supergroup||||
69694|Nullagine Group|67201|5|Briefly described|p12 Tb.1|||Pilbara Craton, De Grey Superbasin, Mosquito Creek Basin.|||Mosquito Creek Formation|||
69694|Nullagine Group|68284|6|Mentioned|p4|||Crops out in the Marble Bar-Nullagine area, East Pilbara Terrane.|2980-2930 Ma.|||||
69694|Nullagine Group|69167|6|Mentioned|geologyp_lut.csv|Mesoarchean|Mesoarchean|||De Grey Supergroup|Includes Mosquito Creek Formation, Coondamar Formation|||
69694|Nullagine Group|69185|4|Described|500k_geologyp08_lut.csv|Mesoarchean|Paleoarchean|Geological Province: Pilbara Craton.||Unit of De Grey Supergroup.|Includes Mosquito Creek Formation.||Psammite and pelite, interbedded|
69694|Nullagine Group|69301|4|Described|p9 Tb.1, p14, p20 Tb.2, p21 Fig.8|||Pilbara Craton. Mosquito Creek Basin. |2930 Ma Mosquito Creek Formation|De Grey Supergroup|Mosquito Creek Formation, Coondamar Formation|||
69694|Nullagine Group|69590|5|Briefly described|GEOL_LUT_CSV files|||Geological province: Pilbara Craton. Of Mosquito Creek Basin. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_geologyp08_lut.csv.||Unit of De Grey Supergroup.|Includes Coondamar Formation, Mosquito Creek Formation.|||
69694|Nullagine Group|70022|6|Mentioned|p113-114, 116|||Mosquito Creek Basin, Pilbara Craton.|3015-2930 Ma.|De Grey Supergroup.|Mosquito Creek Formation.|||
69694|Nullagine Group|70775|5|Briefly described|p12, p38|Mesoarchean||Mosquito Creek Basin.|< 2980 Ma|De Grey Supergroup|Includes the Mosquito Creek Formation.|Overlies the Croydon Group.||
69694|Nullagine Group|70826|6|Mentioned|p6 tbl 2, p8|Mesoarchean|Mesoarchean|Mosquito Creek Basin.||||||
69694|Nullagine Group|72034|6|Mentioned|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Mosquito Creek Formation, Coondamar Formation.|||
69694|Nullagine Group|72668|5|Briefly described|p3, p4, p13, p15|||Mosquito Creek Basin.|c. 2930-2910 Ma|De Grey Supergroup|Includes the Coondamar Formation and the Mosquito Creek Formation.|||13-JAN-22
33830|Nullagine Supersequence|22546|4|Described|359||Archean|Overlies the Lalla Rookh Supersequence. Age of base dated at 2775 Ma.||||||07-NOV-08
33830|Nullagine Supersequence|22682|5|Briefly described|Fig20,p29|Archean|Archean|2772-2725 Ma. Hamersley Province||||||07-NOV-08
33830|Nullagine Supersequence|64724|5|Briefly described|p42|Neoarchean|Neoarchean|Hamersley Basin sedimentary sequence. Age of ~2775 - 2740 Ma from Blake (1993, 2001).||||||
33830|Nullagine Supersequence|65825|6|Mentioned|p20.|Neoarchean|Neoarchean|Named by Blake and Barley (1992), referring to rocks included in the Fortescue Group.||||||
33830|Nullagine Supersequence|65827|6|Mentioned|p33 Fig.7|||Shown as including Kylena and Hardey Formations and Mount Roe Basalt.||||||21-JAN-22
33830|Nullagine Supersequence|66685|6|Mentioned|p217|Archean|Archean|Blake and Barley (1992).||||||
77576|Nullara Sequence|65486|5|Briefly described|p4|Famennian|Fammenian|Second-order Sequence. Overlies Pillara Sequence unconformably; is overlain unconformably by Fairfield Group.||||||
77576|Nullara Sequence|66127|4|Described|p21 Fig.21, pp65-81, p209.|Famennian|Famennian|Second-order sedimentary sequence. Average thickness about 200 m, deposited in c. 11.5 m.y. Includes upper Virgin Hills and Piker Hills Formations, Windjana and Nullara Limestones. Platform-building role performed almost entirely by microbes. Sea level fall led to karstification, with Fairfield Group shales infilling valleys and cavities.||||Overlies Pillara Sequence. Is overlain by Fairfield Group.||
77576|Nullara Sequence|67131|6|Mentioned|p5|Famennian|Famennian|Reef complexes survived the late Famennian mass extinction event and flourished, though with different reef builders, during this depositional episode. Post-Famennian. Shown p3, p4 as Nullara Sequence 1 and Nullara Sequence 2. Both sequences together shown as equivalent to the Nullara Limestone.||||||03-FEB-20
77576|Nullara Sequence|69312|6|Mentioned|p3, p19, p23 fig 27|Famennian|Frasnian|Canning Basin. See also p19, Nullara Limestone p9, Nullara Formation p15.||||Overlies the Pillara Sequence. Overlain by the Fairfield Group.|Carbonates.|11-FEB-20
25355|Nullarbor Limestone|22485|5|Briefly described|p51 , Fig 2|Tertiary|Tertiary|||||||
25355|Nullarbor Limestone|22587|6|Mentioned|p79 Fig. 7|Middle Miocene||||||||
25355|Nullarbor Limestone|22814|5|Briefly described|p258, fig2|Tertiary|Tertiary|||||||
25355|Nullarbor Limestone|23488|6|Mentioned|p39|Miocene|Miocene|Geological Province: Eucla Basin.||||||
25355|Nullarbor Limestone|23671|6|Mentioned|p1|||Overlies the Pidinga Formation.||||||
25355|Nullarbor Limestone|23768|5|Briefly described|p28 Fig.5|Middle Miocene|Middle Miocene|Geological Province: Eucla Basin.  See also p19, p185-187.||||||10-MAR-05
25355|Nullarbor Limestone|23818|4|Described|p174 Fig.84, p198|Early Miocene|Early Miocene|Geological Province: Eucla Basin. Underlain by Wilson Bluff Limestone. Max. thickness: 100 ft.||||||14-MAY-07
25355|Nullarbor Limestone|24057|5|Briefly described|p97|Middle Miocene|Middle Miocene|Geological Basin: Eucla Basin.||||||
25355|Nullarbor Limestone|24201|5|Briefly described|p373 Fig. 2|Oligocene|Eocene|||||||
25355|Nullarbor Limestone|24338|5|Briefly described|p938 Fig. 2|Rupelian|Lutetian|Overlies the Pidinga Formation. Geological Province: Bight Basin.||||||
25355|Nullarbor Limestone|24347|5|Briefly described|p114|Middle Miocene|Middle Miocene|Geological Province: Eucla Basin.||||||
25355|Nullarbor Limestone|24350|5|Briefly described|Fig. 4 Appdx|Oligocene|Eocene|Part of the Dugong Supersequence.||||||
25355|Nullarbor Limestone|24396|5|Briefly described|p222 Fig. 5, p228|Early Pliocene|Middle Miocene|Age: 15.5-5Ma.||||||24-FEB-10
25355|Nullarbor Limestone|24553|5|Briefly described|Figs. 7,8 and 10|Recent|Late Eocene|Along with Wilson Bluff Limestone, equivalent to the Dugong Supersequence.||||||21-JAN-16
25355|Nullarbor Limestone|24606|5|Briefly described|p956, p958 Fig. 3|Early Pliocene|Middle Miocene|Geological Province: Eucla Basin||||||
25355|Nullarbor Limestone|29550|6|Mentioned|p44|||Tertiary||||||
25355|Nullarbor Limestone|29591|5|Briefly described|p92|||||||||
25355|Nullarbor Limestone|29856|6|Mentioned|p37|||||||||
25355|Nullarbor Limestone|30012|5|Briefly described|p20|||Mention Table 1.||||||
25355|Nullarbor Limestone|30268|6|Mentioned|p44|||||||||
25355|Nullarbor Limestone|30514|6|Mentioned|p103|||||||||
25355|Nullarbor Limestone|30563|4|Described|p13|||See stratigraphic table on p6.||||||21-JAN-16
25355|Nullarbor Limestone|30564|5|Briefly described|p12|||||||||
25355|Nullarbor Limestone|30807|6|Mentioned|p101|||Suggested map symbol||||||
25355|Nullarbor Limestone|30917|6|Mentioned|p55|||||||||
25355|Nullarbor Limestone|30922|6|Mentioned|Map legend|Miocene|Miocene|||||||
25355|Nullarbor Limestone|30945|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
25355|Nullarbor Limestone|30952|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
25355|Nullarbor Limestone|30953|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
25355|Nullarbor Limestone|30954|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
25355|Nullarbor Limestone|30962|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
25355|Nullarbor Limestone|30967|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
25355|Nullarbor Limestone|30974|6|Mentioned|Map legend|middle Miocene|middle Miocene|||||||
25355|Nullarbor Limestone|30975|6|Mentioned|Map legend|middle Miocene|middle Miocene|||||||
25355|Nullarbor Limestone|30976|6|Mentioned|Map legend|middle Miocene|middle Miocene|||||||
25355|Nullarbor Limestone|31318|5|Briefly described|p166|||L. Miocene||||||
25355|Nullarbor Limestone|31320|6|Mentioned|p55|||||||||
25355|Nullarbor Limestone|31562|5|Briefly described|p13|||||||||
25355|Nullarbor Limestone|31845|6|Mentioned|p6|||||||||
25355|Nullarbor Limestone|31850|4|Described|p37|||Definition summary.||||||21-JAN-16
25355|Nullarbor Limestone|31902|4|Described|Table 1|||Fig.1||||||
25355|Nullarbor Limestone|31903|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
25355|Nullarbor Limestone|31904|4|Described|p8|||See also Table 1. Refers previous authors||||||
25355|Nullarbor Limestone|31906|4|Described|p8|||Refers previous authors. Table 1||||||
25355|Nullarbor Limestone|31907|4|Described|Table 1|||See also p8,9, Fig.1||||||21-JAN-16
25355|Nullarbor Limestone|31908|4|Described|Table 1|||L.Miocene||||||
25355|Nullarbor Limestone|31909|3|Fully described|p8|||Table 1. Fig.1||||||
25355|Nullarbor Limestone|31913|4|Described|Table 1|||See also Table 1||||||
25355|Nullarbor Limestone|31914|6|Mentioned|Pl.10|||||||||
25355|Nullarbor Limestone|31915|6|Mentioned|Map legend|middle Miocene|middle Miocene|||||||
25355|Nullarbor Limestone|31919|6|Mentioned|p39|||||||||
25355|Nullarbor Limestone|31923|6|Mentioned|p18|||||||||
25355|Nullarbor Limestone|31924|6|Mentioned|p2|||Refers Singleton (1954)||||||
25355|Nullarbor Limestone|32201|5|Briefly described|p6|||See also p7. Refraction survey.||||||21-JAN-16
25355|Nullarbor Limestone|32552|2|Defined|p87|early Miocene|early Miocene|See also p88.||||||21-JAN-16
25355|Nullarbor Limestone|32648|6|Mentioned|p32|||Miocene||||||
25355|Nullarbor Limestone|32750|4|Described|p306|||||||||
25355|Nullarbor Limestone|33586|4|Described|Table 1|||See also p15.||||||21-JAN-16
25355|Nullarbor Limestone|33589|4|Described|p11|||See also p12. M.Miocene.||||||21-JAN-16
25355|Nullarbor Limestone|34180|6|Mentioned|p229|||Miocene||||||
25355|Nullarbor Limestone|34192|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
25355|Nullarbor Limestone|34194|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
25355|Nullarbor Limestone|34232|6|Mentioned|p76|||Irregular cavities.||||||
25355|Nullarbor Limestone|34295|6|Mentioned|p38|||Fauna||||||
25355|Nullarbor Limestone|34308|5|Briefly described|p198|||Batesfordian - Balcombian. See Fig.84||||||
25355|Nullarbor Limestone|34615|6|Mentioned|p10|||||||||
25355|Nullarbor Limestone|34759|6|Mentioned|p60|||||||||
25355|Nullarbor Limestone|34958|6|Mentioned|p88|||||||||
25355|Nullarbor Limestone|35051|6|Mentioned|p204|||Analysis.||||||
25355|Nullarbor Limestone|35059|6|Mentioned|Table.19|||||||||
25355|Nullarbor Limestone|35097|6|Mentioned|p16|||||||||
25355|Nullarbor Limestone|35496|6|Mentioned|p23|||||||||
25355|Nullarbor Limestone|35772|4|Described|Table 1|||||||||
25355|Nullarbor Limestone|36200|6|Mentioned|p6|||||||||
25355|Nullarbor Limestone|36257|6|Mentioned|Table 2.1|||||||||
25355|Nullarbor Limestone|36890|3|Fully described|p415|||||||||
25355|Nullarbor Limestone|37132|5|Briefly described|p369|||||||||
25355|Nullarbor Limestone|37577|6|Mentioned|p75|||||||||
25355|Nullarbor Limestone|37852|6|Mentioned|Fig.3|||||||||
25355|Nullarbor Limestone|38016|6|Mentioned|p88|||||||||
25355|Nullarbor Limestone|38018|6|Mentioned|p124|||||||||
25355|Nullarbor Limestone|38068|6|Mentioned|Fig.7|||||||||
25355|Nullarbor Limestone|38553|6|Mentioned|p43|||||||||
25355|Nullarbor Limestone|38602|6|Mentioned|p2|||||||||
25355|Nullarbor Limestone|40003|5|Briefly described|Table 14|||See also Plate 18||||||
25355|Nullarbor Limestone|40298|6|Mentioned|Table II|||||||||
25355|Nullarbor Limestone|40410|6|Mentioned|p4|||||||||
25355|Nullarbor Limestone|40425|6|Mentioned|p46|||||||||
25355|Nullarbor Limestone|40466|6|Mentioned|p63|||||||||
25355|Nullarbor Limestone|40643|5|Briefly described|p148|||||||||
25355|Nullarbor Limestone|40992|6|Mentioned|Fig.23|||||||||
25355|Nullarbor Limestone|41043|6|Mentioned|p87|||||||||
25355|Nullarbor Limestone|41075|6|Mentioned|p18|||||||||
25355|Nullarbor Limestone|41505|6|Mentioned|p2|||||||||
25355|Nullarbor Limestone|41609|5|Briefly described|Fig.5|||||||||
25355|Nullarbor Limestone|42075|5|Briefly described|Fig.10 P250|||||||||
25355|Nullarbor Limestone|42265|5|Briefly described|p4|||||||||
25355|Nullarbor Limestone|42335|4|Described|p326|||||||||
25355|Nullarbor Limestone|42356|5|Briefly described|Fiche 7 P13|Miocene||||||||
25355|Nullarbor Limestone|42959|5|Briefly described|p58 Fig.3|||||||||
25355|Nullarbor Limestone|43026|5|Briefly described|Table 4,p590|||||||||
25355|Nullarbor Limestone|43040|6|Mentioned|p861|||||||||
25355|Nullarbor Limestone|43053|5|Briefly described|Map Legend|Miocene|Eocene|Geological Province: Eucla Basin.||||||25-MAY-05
25355|Nullarbor Limestone|43203|5|Briefly described|Map Legend||Miocene|Eucla Basin||||||
25355|Nullarbor Limestone|43258|5|Briefly described|Map Legend|Miocene|Eocene|||||||
25355|Nullarbor Limestone|43298|5|Briefly described|Map Legend|Miocene|Eocene|||||||
25355|Nullarbor Limestone|43498|5|Briefly described|8||Miocene|||||||
25355|Nullarbor Limestone|43713|5|Briefly described|p2||Miocene|||||||
25355|Nullarbor Limestone|43814|6|Mentioned|Fig.3,p115|||||||||
25355|Nullarbor Limestone|44133|5|Briefly described|p184, 180 Fig. 10.22|Middle Miocene|Middle Miocene|Geological Province: Eucla Basin. Overlies: Wilson Bluff Limestone. Thickness: 45m. Includes: Mullamullang Member.||||||
25355|Nullarbor Limestone|44145|4|Described|p550, p556-7, p555 fig 4-194, p548|Early Miocene|Early Miocene|Eucla Basin. Age from echinoid and foraminifera fauna. Max known thickness 31m. Type section at Wilson Bluff, east of Eucla.|||Mullamullang Limestone Member|Grades laterally northwards into Colville Sandstone and Plumridge Formation.|Bioclastic calcarenite, locally shelly.|08-OCT-15
25355|Nullarbor Limestone|44365|5|Briefly described|map legend|Pleistocene|Pliocene|||||||
25355|Nullarbor Limestone|44412|14|Not recorded|map legend||Early Miocene|L.Miocene.||||||
25355|Nullarbor Limestone|44695|5|Briefly described|Map Legend|Miocene|Miocene|(Early-Middle Miocene)||||||
25355|Nullarbor Limestone|44864|5|Briefly described|Map Legend||Miocene|||||||
25355|Nullarbor Limestone|45149|4|Described|p63|||||||||
25355|Nullarbor Limestone|46993|6|Mentioned|p262|||||||||
25355|Nullarbor Limestone|60953|5|Briefly described|Map Legend|Miocene|Eocene|Geological Province: Eucla Basin.||||||
25355|Nullarbor Limestone|61108|5|Briefly described|map legend|Miocene|Eocene|Geological Province: Eucla Basin.||||||
25355|Nullarbor Limestone|61155|5|Briefly described|p4, p17|Middle Miocene|Early Miocene|Partly overlies and interfingers with Colville Sandstone. Age: 18.5-14.5Ma. Max. thickness: 40m. Geological Province: Eucla Basin.||||||
25355|Nullarbor Limestone|61197|5|Briefly described|p473, p475, p478 Fig.4, p488-489|Middle Miocene|Early Miocene|Eucla Basin. Marine, shallow shelf deposits. 0-15m thick.|||||Well-cemented, foraminiferal and coralline algal calcarenite.|
25355|Nullarbor Limestone|61234|4|Described|p6, p7 Fig 4.|Early Pliocene|Middle Miocene|Unconformably overlies Wilson Bluff Limestone. Geological Province: Eucla Basin. Marine limestone.||||||14-MAY-07
25355|Nullarbor Limestone|61517|6|Mentioned|p312|||||||||27-MAY-06
25355|Nullarbor Limestone|61544|6|Mentioned|p367 Fig.3. |Eocene|Eocene|||||Overlies Pidinga Formation.||
25355|Nullarbor Limestone|62369|5|Briefly described|p409, p410 Fig.4|Middle Miocene|Early Miocene|Hard, fossiliferous, muddy limestone. Overlies the Abrakurrie Limestone. Geological Province: Eucla Basin.||||||
25355|Nullarbor Limestone|62640|5|Briefly described|pp70-77.     |Miocene|Miocene|Numerous large benthic fauna and relatively high proportion of aragonitic components indicate warmer-water conditions.|||Includes Mullamullang Member.|Overlies Abrakurrie Limestone.|Includes large benthic foraminifera and aragonitic material; well-cemented.|
25355|Nullarbor Limestone|65942|2|Defined|p77-78||Miocene|||Of Eucla Group.||||
25355|Nullarbor Limestone|66131|6|Mentioned|p242 Fig.2|Miocene|Miocene|Early to Middle Miocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||||||
25355|Nullarbor Limestone|67117|5|Briefly described|Map legend.|Miocene|Eocene|Shown under general heading of 'Eocene - Miocene'. Covers over 99% of the map area.|||||Limestone, bioclastic, micritic; subtidal, platformal, above fair-weather wave-base.|03-MAY-13
25355|Nullarbor Limestone|67462|5|Briefly described|Map legend.|Miocene|Miocene|Bunda Plateau, Eucla Basin.||||||
25355|Nullarbor Limestone|67789|5|Briefly described|p33-36, 39, 41-46|Miocene|Miocene|Eucla Basin. Up to 45m thick. Forms the surface of the Nullarbor Plain. Contains shallow caves (tubes and vertical shafts/chambers) across the entire Plain. Comprises an estimated c.25% microkarst cavities (described).||Eucla Group.||Overlies Abrakurrie Limestone. Is overlain locally by Roe Calcarenite.|A hard, abundantly fossiliferous (listed) sub-tropical deposit. Laterally extensive grainstone to rudstone, extensively cemented by diagenetic low-Mg calcite spar. Lithologies described in detail.|
25355|Nullarbor Limestone|67921|5|Briefly described|Map legend|Pliocene|Miocene|Subcrop and minor outcrop.|||||Marine platform bioclastic limestone. Indurated and recrystallised with basal member of mud, sand and grit. Lagoonal, calcareous and dolomitic mudstone as at Ifould Lake. Lower part may be distinctly echinoidal. Upper part is foraminiferal.|
25355|Nullarbor Limestone|69004|5|Briefly described|p19, p34, p41, p115|Middle Miocene|Lower Miocene|Eucla Basin. Up to 25m thick in the Iluka Palaeovalley. Has restricted distribution in the Eucla Basin.||||Overlies the Pidinga Formation.|Carbonates including limestone.|
25355|Nullarbor Limestone|69297|5|Briefly described|p14 fig 2.4|Holocene|Lutetian|Eyre, Ceduna and Duntroon Sub-basins. See also p25 fig 2.9, p39 fig 2.14, p60.||||Overlies the Pidinga Formation.|Limestones.|
25355|Nullarbor Limestone|69386|6|Mentioned|p7|Miocene|Miocene|Eucla Basin.||||||
25355|Nullarbor Limestone|69598|5|Briefly described|p2, p9, p10, p11 Tb.1, p29 Tb.4|Pliocene|Middle Miocene|Eucla Basin. Up to 35m thick. Potential carbon dioxide storage reservoir.||||Overlies the Abrakurrie Limestone. Grades into and interfingers with the Colville Sandstone and Plumridge Formation.|Marine carbonates including limestone and foraminiferal algal calcarenites and rhodolith rudstones to floatstones.|
25355|Nullarbor Limestone|69632|5|Briefly described|p26-27, p30, p32|Miocene|Miocene|Eucla Basin. Early to middle Miocene. Most lithified unit in the Group, due to low-Mg calcite cement. Has extensive secondary porosity.||Eucla Group|||Limestone rich in coralline algae (rhodoliths and articulated types), large and small benthic foraminifera, and molluscs.|09-OCT-18
25355|Nullarbor Limestone|69648|4|Described|p4,p6 Fig.3,p20 Plate3,p23,p25-27,p32-33|Miocene|Miocene|Basement highs with thin cover. Semi-arid - arid karst region: immature karst. Nullabor Plain, Eucla Basin. Age: deposited early Middle Miocene. Marine platform bioclastic carbonates; locally at base is thin (20-30 cm) transgressive lag (v.poorly sorted, non-calcareous, clay, sand, grit); basal 1-2 m limestone (trace quartz grains); most of overlying limestone has no terrigenous clastic component; mostly foraminifera-rich packstone. Best exposed on cliffs of Great Australian Bight and in quarries (~12 m at Watson). Overall uniformity of thickness (20-35 m) across platform, that extends beneath dunefield. See also map legend.|~15 Ma|Eucla Group||Overlies palaeochannels of Pidinga Formation; no evidence of intertonguing with Hampton Sandstone; sharply overlies Yarle Sandstone.|Locally thin base of terrigenous lag (20-30 cm), basal (1-2 m) limestone (trace quartz), no terrigenous component to most of overlying limestone; predominantly indurated, recrystallised, micritic, bioclastic, white, off-white to grey limestone.|
25355|Nullarbor Limestone|70067|6|Mentioned|Ceduna: Fig.2. Regional: Fig.2|Holocene|Eocene|Bight Basin.||||||
25355|Nullarbor Limestone|70337|5|Briefly described|Map legend.|Miocene|Eocene||||||Limestone, bioclastic, micritic. Subtidal, platformal, above fair-weather wave-base.|
25355|Nullarbor Limestone|70397|4|Described|p1-8,10-13|Middle Miocene|Middle Miocene|Eucla Basin. Extremely fossiliferous; contains large benthic foraminifera and zooxanthellate corals. Comprises five main facies and subfacies. See p3-11 for detailed lithofacies descriptions. See also Table 1 p6 for summary. Deposition coincides with the Miocene Climatic Optimum, a time of elevated temperatures worldwide that caused expansion of tropical waters and associated organisms into higher latitudes (McGowran et al., 1997b).||Unit of Eucla Group.|Includes Rawlinna member and Mullamullang Member.|Onlaps on Abrakurrie Limestone and Wilson Bluff limestone (inboard). Laterally grades inboard (N-ward) into Colville Sandstone. Overlies the Eucla Group. Unconformably overlain by the Roe Calcarenite.|Rhodolith Facies, Articulated Coralline Algae Facies, Benthic Foraminifera Facies, Echinoid Facies, and Planktonic Foraminifera Facies.|29-JUL-19
25355|Nullarbor Limestone|70771|4|Described|p3-p4, p7, p11-p13, p15, p21, p27|Middle Miocene|Early Miocene|Eucla Platform, Eucla Basin.  [The author assigns this unit to the Eucla Group however this term is obsolete]. See also p31, p33, p39-p40, p53-p58, p60-p61.||Eucla Group|Includes the Mullamullang Member.|Disconformably overlies the Abrakurrie Limestone.||
25355|Nullarbor Limestone|70778|5|Briefly described|p4, p10|||Intersected in Nundroo 3 DDH.|||||Limestone, calcareous mudstone.|
25355|Nullarbor Limestone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||limestone, calcarenite|
25355|Nullarbor Limestone|71361|4|Described|ii, p1-p3, p5-p6, p15, p17-p20, |Middle Miocene|Early Miocene|Eucla Basin. [NB that the Eucla Group to which the author assigns this unit is currently in disuse]. This unit has a rich fossil assemblage containing coralline algae, large and small benthic foraminifera and molluscs; diverse zooxanthellate corals are also present but not numerous. Fossil assemblage, palaeoenvironments and facies are discussed in great detail. This unit is interpreted to have been deposited in three main palaeoenvironments: rhodolith gravels, seagrass banks and open seafloors. See also p22-p23, p25-p28, p31, p33-p34, p37, p39, p41-p51, p53-p81, p117, p119-p120, p122-p123, p129, p135, p137-p145, p148-p160.||Eucla Group|Includes the Mullamullang Limestone Member.|Unconformably overlies the Wilson Bluff Limestone and the Abrakurrie Limestone. Unconformably overlain by the Roe Calcarenite. Equivalent to (grades into) the Colville Sandstone.|Fine to coarse grained fossiliferous calcarenites.|
25355|Nullarbor Limestone|71618|6|Mentioned|p124|Cenozoic|Cenozoic|Geological province: Eucla Basin.||Unit of Eucla Group.||||
25355|Nullarbor Limestone|71758|14|Not recorded|p81|||In 1967 Annual Report.||||||
25355|Nullarbor Limestone|71891|5|Briefly described|p6-p7, p14, p29-p52, p54-p55|Cenozoic|Cenozoic|Eucla Basin, Coompana Province. 20-35m thick unit interpreted to have been deposited in a shallow platform setting with a paucity or terrigenous material suggesting river systems carried little debris to the coast.||||Overlies the Abrakurrie Limestone.|Hard, chalky limestone.|
25355|Nullarbor Limestone|72344|5|Briefly described|p5, p16, p49, p61|||Eucla Basin. 20-35m thick. Includes large benthic foraminifera and aragonitic material. Interpreted to have been deposited in a shallow platform setting with the paucity of terrigenous material suggesting river systems carried little debris to the coast. See also p84, p96, p160, p169.||||Overlies the Abrakurrie Limestone.|Limestone, bioclastic, micritic subtidal, platformal, above fair weather wave-base.|
25355|Nullarbor Limestone|72465|5|Briefly described|p9, 15, 17|Tertiary|Tertiary|Eucla Basin, Coompana Province. 20-35m thick. Forms the ""lumpy"" brown, parallel-bedded unit at the top of the Bunda Cliffs.||||Overlies Abrakurrie Limestone.|Limestone, bioclastic, micritic. Subtidal, platformal, above fair-weather wave-base. Includes large benthic foraminifera and aragonitic material, well-cemented.|
25355|Nullarbor Limestone|72466|5|Briefly described|p9, 15, 17|Tertiary|Tertiary|Benbow et al. (1995). Eucla Basin, Coompana Province. 20-35m thick. Deposited in a shallow platform setting. Forms the ""lumpy"" brown, parallel-bedded unit at the top of the Bunda Cliffs.||||Overlies Abrakurrie Limestone.|Limestone, bioclastic, micritic, subtidal, platformal, above fair-weather wave-base. Includes benthic foraminifera and aragonitic material; well-cemented.|
25355|Nullarbor Limestone|72467|5|Briefly described|p9, p15, 17|Tertiary|Tertiary|Eucla Basin, Coompana Province. 20-35m thick. Forms the ""lumpy"" brown, parallel-bedded unit at the top of the Bunda Cliffs.||||Overlies Abrakurrie Limestone.|Limestone, bioclastic, micritic. Subtidal, platformal, above fair-weather wave-base. Includes large benthic foraminifera and aragonitic material, well-cemented.|
25355|Nullarbor Limestone|72468|5|Briefly described|p9, p15, p17|||Eucla Basin. 20-35 m thick. Deposited in a shallow platform setting, with the paucity of terrigenous material suggesting river systems carried little debris to the coast. Forms the 'lumpy' brown, parallel-bedded unit at the top of the Bunda Cliffs.||||Underlain by Abrakurrie Limestone.|Limestone, bioclastic, micritic. Subtidal, platformal, above fair weather wave-base. Includes large benthic foraminifera and aragonitic material; well-cemented.|
25355|Nullarbor Limestone|72469|5|Briefly described|p9, p15, p17|||Eucla Basin. 20-35 m thick. Deposited in a shallow platform setting, with the paucity of terrigenous material suggesting river systems carried little debris to the coast. Forms the 'lumpy' brown, parallel-bedded unit at the top of the Bunda Cliffs.||||Underlain by Abrakurrie Limestone.|Limestone, bioclastic, micritic. Subtidal, platformal, above fair weather wave-base. Includes large benthic foraminifera and aragonitic material; well-cemented.|
25355|Nullarbor Limestone|72470|5|Briefly described|p9, p15, p18|||Eucla Basin. 20-35 m thick. Deposited in a shallow platform setting, with the paucity of terrigenous material suggesting river systems carried little debris to the coast. Forms the 'lumpy' brown, parallel-bedded unit at the top of the Bunda Cliffs.||||Underlain by Abrakurrie Limestone.|Limestone, bioclastic, micritic. Subtidal, platformal, above fair weather wave-base. Includes large benthic foraminifera and aragonitic material; well-cemented.|
25355|Nullarbor Limestone|72471|5|Briefly described|p9, p15, p17|||Eucla Basin. 20-35 m thick. Deposited in a shallow platform setting, with the paucity of terrigenous material suggesting river systems carried little debris to the coast. Forms the 'lumpy' brown, parallel-bedded unit at the top of the Bunda Cliffs.||||Underlain by Abrakurrie Limestone.|Limestone, bioclastic, micritic. Subtidal, platformal, above fair weather wave-base. Includes large benthic foraminifera and aragonitic material; well-cemented.|
25355|Nullarbor Limestone|72472|5|Briefly described|p9, p15-16|||Eucla Basin. 20-35 m thick. Deposited in a shallow platform setting, with the paucity of terrigenous material suggesting river systems carried little debris to the coast. Forms the 'lumpy' brown, parallel-bedded unit at the top of the Bunda Cliffs.||||Underlain by Abrakurrie Limestone.|Limestone, bioclastic, micritic. Subtidal, platformal, above fair weather wave-base. Includes large benthic foraminifera and aragonitic material; well-cemented.|
25355|Nullarbor Limestone|73084|5|Briefly described|p16-17|Eocene|Eocene|Eucla Basin||||Underlain by Wilson Bluff Limestone.|Hard, chalky limestone.|
25355|Nullarbor Limestone|73101|5|Briefly described|Map legend.|Miocene|Eocene||||||Limestone, bioclastic, micritic. Subtidal, platformal, above fair-weather wave-base.|
25355|Nullarbor Limestone|73108|5|Briefly described|Map legend.|Miocene|Eocene||||||Limestone, bioclastic, micritic. Subtidal, platformal, above fair-weather wave-base.|
25355|Nullarbor Limestone|73112|5|Briefly described|Map legend.|Miocene|Miocene|||||Locally overlies Abraukurrie Limestone.|Yellow-brown, hard, recrystallised fossiliferous limestone|
25355|Nullarbor Limestone|73641|5|Briefly described|p5-11, 13-15|Miocene|Miocene|Eucla Basin. 20-35m thick. Subtidal, above wave-base, deposits. Features numerous large caves, karst pocket valleys, and thousands of sub-metre scale blowholes. Local calcrete induration to the SE. Is blanketed by 10-20 cm thick layer of calcareous soil. Photographs. Mineralogical, elemental, TOC compositions tabulated.||||Overlies Abrakurrie Limestone.|Bioclastic micritic limestone.|
38012|Numbana Monzogranite|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Age:<2930Ma (Blewett et al, 2001). Geological Province: Pilbara Craton.||||||15-APR-13
38012|Numbana Monzogranite|24110|5|Briefly described|Plate 1|Archean|Archean|Belongs to Yule Granitoid Complex. Geological Province: Pilbara Craton.||||||15-APR-13
38012|Numbana Monzogranite|24193|5|Briefly described|p874, p877 Tb.1, p890|Archean|Archean|Of the Yule granitoid complex. Geological Province: Pilbara Craton. Age: 2.93-2.85Ga.||||||07-NOV-08
38012|Numbana Monzogranite|50379|5|Briefly described|Map Legend|Archean|Archean|Of Yule Granitoid Complex. Geological Province: Pilbara Craton.||||||07-NOV-08
38012|Numbana Monzogranite|63441|5|Briefly described|p12 Tb. 2|Archean|Archean|Of Split Rock Supersuite. Geological Province: Pilbara Craton.||||||15-APR-13
38012|Numbana Monzogranite|64580|4|Described|map legend||Mesoarchean|Of Split Rock Supersuite. Medium- to coarse-grained feldspar(-quartz) porphyritic monzogranite; massive to weakly foliated; local flow-aligned feldspar phenocrysts; local garnet-bearing pegmatite and granite dykes.||||||15-DEC-08
38012|Numbana Monzogranite|66108|5|Briefly described|Map legend|Neoarchean|Neoarchean|Unit in Split Rock Supersuite. Medium- to coarse-grained feldspar(-quartz) porphyritic monzogranite; massive to weakly foliated; local flow-aligned feldspar phenocrysts; local garnet-bearing pegmatite and granite dykes.||||||
38012|Numbana Monzogranite|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton. Age constrained by the parent Split Rock Supersuite. Locally abundant pegmatite and leucogranite of the Numbana Monzogranite occurs within Mungarinya Monzogranite (Sisters Supersuite). Includes 6 separately mapped sub-units: see map legend for lithological details.||Of the Split Rock Supersuite.|||Medium- to coarse-grained feldspar(-quartz) porphyritic monzogranite; massive to weakly foliated; local flow-aligned feldspar phenocrysts; local garnet-bearing pegmatite and granite dykes.|30-APR-14
38012|Numbana Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Porphyritic monzogranite; massive to weakly foliated; local flow-aligned feldspar phenocrysts; local garnet-bearing pegmatite and granite dykes. Biotite-muscovite monzogranite, porphyritic-equigranular monzogranite. Biotite-muscovite leucogranite.|
38012|Numbana Monzogranite|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Split Rock Supersuite.|||Medium- to coarse-grained feldspar(-quartz) porphyritic monzogranite; massive to weakly foliated; local flow-aligned feldspar phenocrysts; local garnet-bearing pegmatite and granite dykes|
38012|Numbana Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; Split Rock Supersuite Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|2851-2831 Ma (inferred)|Unit of Split Rock Supersuite.|||Biotite(-muscovite)(-garnet) monzogranite; feldspar porphyritic; garnet-bearing pegmatites and granite dykes; rafts of Pincunah Monzogranite.|
38012|Numbana Monzogranite|71041|5|Briefly described|p45, p47 fig 4|Neoarchean|Mesoarchean|Intrusion of pegmatite dykes of this unit produced the Wodgina tantalum-tin deposits. |2870 +/- 90 Ma|Of Split Rock Supersuite.|||Monzogranite, pegmatite dykes.|10-NOV-17
38012|Numbana Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, granite|
38012|Numbana Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Medium- to coarse-grained feldspar(--quartz) porphyritic monzogranite; massive to weakly foliated; local flow-aligned feldspar phenocrysts; local garnet-bearing pegmatite and granite dykes.|
26085|Nurina Formation|22663|5|Briefly described|S97-1 and 2 p3||Late Cretaceous|||||||
26085|Nurina Formation|22814|5|Briefly described|fig2|Cretaceous|Cretaceous|||||||
26085|Nurina Formation|41751|2|Defined|p2|Campanian|Santonian|Age: Santonian to early Campanian.||||||
26085|Nurina Formation|42315|6|Mentioned|p2|Senonian||||||||
26085|Nurina Formation|42545|3|Fully described|p17|Campanian|Santonian|||||||
26085|Nurina Formation|43498|6|Mentioned|8|Santonian|Neocomian|||||||
26085|Nurina Formation|44133|5|Briefly described|p137|Mesozoic|Mesozoic|Maximum Thickness: 53m. Formerly assigned to Madura Formation. ||||||
26085|Nurina Formation|44145|4|Described|p549 fig 4-190, p551, p554-5, p553|Campanian|Santonian|Eucla Basin. Probably equivalent age to Wigunda Formation, Ceduna Terrace. Appears restricted to central part of Eucla Basin, around Madura. Where found, thickness 29-41m. Age based on palynomorphs. Previously included in Madura Formation. Type secion said to be in Transcontinental Railway Bore 1, 283-336m.||||Disconformably overlies Toondi Formation.|Greensand, glauconitic sandstone and sandy siltstone.|08-OCT-15
26085|Nurina Formation|68715|6|Mentioned|p30 Fig.5|Campanian|Santonian|Bight Basin.||||||
31860|O'Callaghans Granite|24197|5|Briefly described|p26, p102 Tb. 14.1|Neoproterozoic|Neoproterozoic|Of O'Callaghans Supersuite. I-type (granodioritic) Minyari type granite. Age: ~625Ma. Geological province: Paterson Province.||||||27-SEP-12
31860|O'Callaghans Granite|43867|6|Mentioned|Fig.8 p203,|||May be intended as an informal name? - O'Callaghan's granite mentioned in text.  Fig.10 p205.||||||19-FEB-08
31860|O'Callaghans Granite|43868|5|Briefly described|p161|||May be similar age to Mount Crofton Granite||||||
31860|O'Callaghans Granite|50436|5|Briefly described|p1.3, 4.1, Table 1.1|Neoproterozoic|Neoproterozoic|Geological Province: Paterson Orogen. Of the Minyari Group (O'Callaghans Supersuite).|||||syenogranite.|27-SEP-12
31860|O'Callaghans Granite|67202|5|Briefly described|p189, p199, p201, p203, p208|||A unit in the Minyari group of granites (a subdivision of the O'Callaghans Supersuite by Goellnicht et al., 1991); assigned to the O'Callaghans Suite by Wyborn (1997) and Budd et al. (2001). Associated with the O'Callaghans W(-Zn-Pb-Cu) deposit (described). Appears as O'Callaghans Group on p203.|650-630 Ma.|O'Callaghans Suite.||Intrudes Puntapunta Formation.||
31858|O'Callaghans Supersuite|24197|4|Described|p26, 27, p100|||Same as O'Callaghan's Supersuite - correct spelling is O'Callaghans Supersuite. Divided into 2 suites: Mount Crofton Suite (oxidised) and O'Callaghans Suite (reduced). Age: ~625Ma. But see O'Callaghan's Supersuite for detail.||||||27-SEP-12
31858|O'Callaghans Supersuite|50436|5|Briefly described|p1.3, 4.1, Table 1.1|Neoproterozoic|Neoproterozoic|Geological Province: Paterson Orogen. Age: ~625Ma. Equigranular even and medium-grained monzogranite to syenogranite which commonly grade into coarse porphyritic textures. Granite compositions are extremely variable.||||||27-SEP-12
31858|O'Callaghans Supersuite|65454|4|Described|p12-13|Cryogenian|Cryogenian|Highly fractionated, I-type monzogranite to syenogranite with varying oxidation states. Emplaced between ~654 and 630 Ma. Intrudes Lamil Group.  Contains Mount Crofton and O'Callaghans Suites.||||||
31858|O'Callaghans Supersuite|67202|4|Described|p155, p189-191, p201, p205-206, p279-281|||Budd et al. (2001). Associated with W-Zn-Pb-Cu and Au-Cu mineralisation. Divided into two groups [sic] by Goellnicht et al. (1991), and more formally into two Suites by  Wyborn (1997) and Budd et al. (2001). Geochemistry.|c.655-630 Ma.||Mount Crofton, O'Callaghans Suites.|Intrudes the Yeneena Supergroup.|Granites.|
31858|O'Callaghans Supersuite|69003|5|Briefly described|p4, p64-65|Neoproterozoic|Neoproterozoic|Paterson Orogen. Intrusions during the Miles Orogeny may be associated with significant Cu-Au mineralisation at Telfer.|655-630 Ma.|||Intrudes the Lamil Group.|Granites.|
31858|O'Callaghans Supersuite|71169|5|Briefly described|p16|Cryogenian|Cryogenian|U-Pb zircon and titanite dates generally fall between 645-625 Ma (Dunphy and McNaughton, 1998; Bagas, 2004; Maidment et al., 2010)|678 +/- 12 Ma (U-Pb Titanite)||||Monzogranite.|
31858|O'Callaghans Supersuite|71795|6|Mentioned|p33 fig 2|Neoproterozoic|Neoproterozoic|||||||
31858|O'Callaghans Supersuite|72258|5|Briefly described|p134|Neoproterozoic|Neoproterozoic|Geological province: Paterson Orogen. Possible source of Neoproterozoic detrital zircons into the Perth Basin.||||||
31858|O'Callaghans Supersuite|73234|6|Mentioned|p20|Ediacaran|Cryogenian|Paterson Orogen, northern.|c. 655-625 Ma|||||
25361|Odjick Formation|41997|6|Mentioned|p72|||||||||
40749|Oldham Sandstone|24183|6|Mentioned|p20|||Equivalent of the Collier Group.||||||
40749|Oldham Sandstone|50188|2|Defined|p9, 15|Mesoproterozoic|Mesoproterozoic|Unconformably underlies Brassey Range Formation. Geological Province: Oldham Inlier. Type area in text.  Max.thickness: 4000m+.  Age: c.1200Ma.||||||17-JUL-08
40749|Oldham Sandstone|64283|5|Briefly described|p49, p51 Fig. 2, p52|Mesoproterozoic|Mesoproterozoic|Previously mapped into former Cornelia Formation. Unconformably overlain by Brassey Range Formation. Age: 1.2? Geological province: Oldham Inlier. Silicified, x-bedded and rippled quartz sandstone; moderately dipping.||||||07-FEB-11
40749|Oldham Sandstone|64286|5|Briefly described|p72, p73 Fig. 1|||Formerly mapped as Cornelia Sandstone together with Quadrio Formation and the current Cornelia Formation. Geological province: Oldham Inlier. Silicified sandstone, moderately dipping. See also p74 Table 1.||||||07-FEB-11
40749|Oldham Sandstone|64580|4|Described|map legend||Mesoproterozoic|Silicified quartz sandstone; with local pebbly lenses.||||||15-DEC-08
40749|Oldham Sandstone|64772|5|Briefly described|p13, p34 Fig. 22, Plate 1, p82,|Mesoproterozoic|Mesoproterozoic|Geological province: Oldham Inlier. Previously included in Cornelia Sandstone/Formation.Silicified quartz sandstone; local pebbly lenses.|<1340 Ma|||||25-NOV-13
40749|Oldham Sandstone|70826|6|Mentioned|p10|Mesoproterozoic|Mesoproterozoic|Ward and Oldham Inliers of the Capricorn Orogen. Deposition may be related to the 1321-1171 Mutherbukin Tectonic event.||||||
40749|Oldham Sandstone|70936|6|Mentioned|p74|||Intersected at the bottom of Lancer-1 drillhole below thick Neoproterozoic succession,~ 600km SSE of Y10 pit.||||||
40749|Oldham Sandstone|71169|5|Briefly described|p80|Ectasian|Calymmian|Ward and Oldham Inliers. Deposited in a deltaic to shallow marine setting; paleocurrents from east and north.|1410-1279 Ma|||||
40749|Oldham Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, conglomerate|
40749|Oldham Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic||Max age 1338+/-27 Ma, min ~1229 Ma.||||Silicified quartz sandstone; with local pebbly lenses.|
78999|Olive Queen Gabbro|70226|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Carton. Eight un-named facies are mapped separately.|c. 2793 Ma.|Warriedar Suite.|||Very coarse grained quartz gabbro with coarse spinifex-like granophyric texture with up to 10 cm crystals; metamorphosed. Also diorite, ultramafic talc-tremolite-serpentine-magnetite schist and peridotite.|16-DEC-15
78999|Olive Queen Gabbro|70796|5|Briefly described|100k_geologyl_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv,  500k_interpgeop_lut.csv. Numerous additional lithologies are discussed.|ca 2793 Ma (inferred)|Warriedar Suite|||Ultramafic talctremoliteserpentinemagnetite schist; locally strongly sheared. Very coarse grained, quartz bearing gabbro, metadolerite to metagabbro, metamorphosed gabbro, quartz gabbro, peridotite, diorite.|
78999|Olive Queen Gabbro|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.|2793+\-4 Ma (isotopic)|Unit of Warriedar Suite.|||Gabbro, layers of leucogabbro, quartz gabbro to diorite, pegmatitic gabbro, and dolerite; metamorphosed; metadolerite, metagabbro; inyerlayered with tremolite-bearing ultramafic schist; peridotite, minor pyroxenite.|
37998|Oliver Sandstone Member|24218|5|Briefly described|p847|Early Miocene|Early Miocene|Of the Oliver Formation. Geological Province: Bonaparte Basin.||||||21-NOV-06
37998|Oliver Sandstone Member|64695|5|Briefly described|p262  |Miocene|Miocene|Northern Bonaparte Basin.||Unit in Oliver Sandstone.||||
37998|Oliver Sandstone Member|65680|6|Mentioned|p709 Fig.2.|Langhian|Aquitanian|||Unit in Oliver Formation.||Unconformably overlies Hibernia Formation.||
37998|Oliver Sandstone Member|69452|5|Briefly described|p36:15|||Bonaparte Basin.||Oliver Formation.||||12-JUL-16
37998|Oliver Sandstone Member|70061|5|Briefly described|Regional geology Figs.6-7. Sahul: Fig.2|Miocene|Oligocene|See also Vulcan: Fig.2, p2.||Oliver Formation.||Equivalent to Cartier Formation.||12-JUL-16
37998|Oliver Sandstone Member|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Miocene|Miocene|See also Northern: Fig.2. Brecknoff-Scott Reef Trend and Caswell-Barcoo Sub-basins, Browse Basin.||Oliver Formation.||||12-JUL-16
30595|Onedin Member|23621|2|Defined|p55 Appendix|Orosirian|Orosirian|See also page 11 table 1. Type Section included. Of Koongie Park Formation. Geological Province: Halls Creek Orogen. Max. thickness: 150 m.||||||
30595|Onedin Member|23622|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Koongie Park Formation.||||||
30595|Onedin Member|24173|4|Described|p19, p13 Tb.2|Paleoproterozoic|Paleoproterozoic|Of the Koongie Park Formation. Geological Province: Halls Creek Orogen. Max Thickness: >150m. Intrudes felsic volcanics dated at c.1843Ma. Hosts copper-lead-zinc deposits||||||07-NOV-08
30595|Onedin Member|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Koongie Park Formation|||Pelite, calc-silicate rock, metachert, and meta-ironstone.|03-AUG-15
30595|Onedin Member|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Koongie Park Formation|||Pelite, calc-silicate rock, metachert, and meta-ironstone|
30595|Onedin Member|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Central Zone.|1845-1840 Ma (Inferred)|Unit of Koongie Park Formation.|||Pelite, calc-silicate rock, metachert, and meta-ironstone|
30595|Onedin Member|70154|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1840-1845 Ma|Koongie Park Formation|||Pelite, calc-silicate rock, metachert and metaironstone.|
30595|Onedin Member|70812|5|Briefly described|p13, p20|||||Koongie Park Formation|||Chemical sedimentary rocks.|
30595|Onedin Member|71267|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (183 -1821 Ma).|1845-1840 Ma (inferred)|Unit of Koongie Park Formation.|||Pelite, calc-silicate rock, metachert, and meta-ironstone|
79853|Opal Gabbro|70830|5|Briefly described|p14-p15|||||||Intrudes the Polelle Group.||
79853|Opal Gabbro|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma).|2735-2711 Ma|Unit of Yalgowra Suite.|||Layered mafic-ultramafic intrusive rocks; dominantly gabbro with minor gabbronorite, leucogabbro, and dolerite, weakly deformed; metamorphosed|
79853|Opal Gabbro|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.||Yalgowra Suite.|||Layered mafic-ultramafic intrusive rocks: dominantly gabbro with minor gabbronorite, leucogabbro and dolerite; weakly deformed, metamorphosed.|
37208|Opaline Well Intrusion|23793|5|Briefly described|p31|||||||||
37208|Opaline Well Intrusion|24024|5|Briefly described|Map Legend|Archean|Archean|Informal name - structural term, not stratigraphic. Of the Pilbara Supergroup. Geological Province: Pilbara Craton.||||||15-DEC-08
37208|Opaline Well Intrusion|63441|5|Briefly described|12 Tb. 2, p38|Archean|Archean|Of Langenbeck Suite. On SHERLOCK.||||||07-FEB-11
37208|Opaline Well Intrusion|64174|5|Briefly described|Map legend|Archean|Archean|Of the Radley Suite (Sisters Supersuite).  Geological province: Mallina Basin.  Gabbro and dolerite; local dunite, peridotite, pyroxenite and basaltic rock; metamorphosed.||||||04-DEC-08
37208|Opaline Well Intrusion|64580|4|Described|map legend||Mesoarchean|Of Langenbeck Suite. Gabbro and dolerite; local dunite, peridotite, pyroxenite, and basaltic rock; metamorphosed.||||||15-DEC-08
37208|Opaline Well Intrusion|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Lagenbeck Suite.|||Gabbro and dolerite; local dunite, peridotite, pyroxenite, and basaltic rock; metamorphosed|
37208|Opaline Well Intrusion|69300|5|Briefly described|map legend|Archean|Archean|Mallina Basin||Pilbara Supergroup|||undivided gabbro, mafic, and ultramafic rocks forming layered sills; metamorphosed|
37208|Opaline Well Intrusion|70775|5|Briefly described|p65, p76|||Interpreted to be an intrusive equivalent to the Louden Volcanics.||||Intrudes the Cistern Formation and the Whim Creek Group.||
37208|Opaline Well Intrusion|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||olivine gabbro, pyroxenite, dunite, basalt|
37208|Opaline Well Intrusion|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Langenbeck Suite|||Gabbro and dolerite; local dunite, peridotite, pyroxenite, and basaltic rock; metamorphosed.|
79353|Ora Banda Gabbro|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2702-2692 Ma (inferred)||||Quartz-bearing gabbro locally grading into granophyre; metamorphosed; gabbronorite; locally minor leucogabbro; metamorphosed; Peridotite; relict olivine orthocumulate texture; commonly serpentinized and locally silicified.|
23887|Orinda Gabbro|42436|6|Mentioned|Fig.2 p75|||Related to Orinda Sill?||||||17-FEB-14
23887|Orinda Gabbro|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).  See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2702-2692 Ma (inferred)||||Gabbro to leucogabbro dominant; locally granophyric; metamorphosed|
83021|Oroya Shale|73300|6|Mentioned|p1113|||Yilgarn Craton, Kalgoorlie terrane.||||Overlies the Paringa Basalt, underlies the Aberdare Dolerite, ?Golden Mile Dolerite, Black Flag Basalt.||
68743|Orpheus Supersuite|63441|3|Fully described|p36, p10 Tb. 2|Archean|Archean|Includes 8 granites including Andover and Bullock Hide Intrusions. Age: 3025-3010Ma. Geological province: Pilbara Craton. See also p32 Fig. 11.||||||07-FEB-11
68743|Orpheus Supersuite|63538|6|Mentioned|p6 Fig. 3|Archaean|Archaean|Geological Province: Pilbara Craton.||||||19-APR-13
68743|Orpheus Supersuite|64174|5|Briefly described|Map legend|Archean|Archean|Includes 8 named granites and 2 named intrusions. Age ranges included: 3021-3015Ma to 3017-3012Ma.  Geological province: Pilbara Craton.||||||07-NOV-08
68743|Orpheus Supersuite|64580|4|Described|map legend||Mesoarchean|Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed.||||||15-DEC-08
68743|Orpheus Supersuite|67201|4|Described|p7 Fig.4, p13 Fig.8, see comments|Archean|Archean|Pilbara Craton. West Pilbara Superterrane. Page location continued: p16-17, p23, p27, p44.|c. 3015 Ma dacite sills; 3025-3010 Ma||Snell Well Granodiorite, Stone Yard Granophyre, Mount Gregory Monzodiorite, Rea Dacite, Black Hill Well Monzogranite, Mount Wangee Dacite, Andover Intrusion|Intrudes Cleaverville Formation. Sills intrude Regal Formation.|Gabbro, granite. Intrusive sheets of porphyry and porphyritic microgranite.|24-NOV-16
68743|Orpheus Supersuite|68035|5|Briefly described|p290 Fig 5|Mesoarchean|Mesoarchean||3.02 - 3.01 Ga||||Monzogranite and dacite; mafic-ultramafic intrusions|
68743|Orpheus Supersuite|69185|4|Described|500k_geologyp08_lut.csv|Mesoarchean|Paleoarchean|Geological Province: Pilbara Craton. Also includes Mount Gregory Monzodiorite, Mount Wangee Dacite, Rea Dacite, Stone Yard Granophyre.|||Includes INTRUSIONS: Andover, Bullock Hide; MONZOGRANITE: Black Hill Well, South Whundo; GRANODIORITE: Forrestier Bay, Snell Well.||Gabbro and dolerite, metamorphosed.|
68743|Orpheus Supersuite|69301|5|Briefly described|p5 Fig.3|||Pilbara Craton. West Pilbara Superterrane.|||||Granitic rocks.|
68743|Orpheus Supersuite|70022|6|Mentioned|p115|||West Pilbara Superterrane.||||||
68743|Orpheus Supersuite|70775|4|Described|iii, p8 fig 5, p9-p10|Mesoarchean|Mesoarchean|Gorge Creek Basin. Intrusion of this supersuite was contemporaneous with deposition of the Cleaverville Formation. This supersuite is interpreted as a precursor to the Maitland River Supersuite on the basis of its marginally older age and similar distribution. Also includes Mount Gregory Monzodiorite, Stone Yard Granophyre, Snell Well Granodiorite, South Whundo Monzogranite and the Forestier Bay Granodiorite. See also p13, p15-p17, p22, p38-p39, p43, p44 fig 27, p46-p51, p66, p73, p81, p94.|c. 3023-3012 Ma||Includes the Andover Intrusion, Mount Wangee Dacite, Black Hill Well Monzogranite, Rea Dacite.|Intrudes the Cleaverville Formation. Intruded by the Maitland River Supersuite.|Mafic-ultramafic and felsic intrusions including gabbro, peridotites and granites.|
68743|Orpheus Supersuite|70826|6|Mentioned|p8|Mesoarchean|Mesoarchean|East Pilbara Terrane and Karratha Terrane.||||||
68743|Orpheus Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|De Grey Superbasin. Divided in to 7 named units and 1 unnamed unit.|Max age 3023+/-9 Ma, min 3012+/-3 Ma||Includes Snell Well Granodiorite, Andover Intrusion, South Whundo Monzogranite, Forestier Bay Granodiorite, Rea Dacite, Mount Gregory Monzodiorite, Mount Gregory Monzodiorite.||Granodiorite, monzogranite, dacite, and granophyre, and ultramafic--mafic intrusive rocks; local monzodiorite; metamorphosed. Gabbro, leucogabbro, serpentinized peridotite and dunite, pyroxenite, and minor anorthosite; metamorphosed.|
68743|Orpheus Supersuite|72251|6|Mentioned|p54|||Geological province: West Pilbara Superterrane, Pilbara Craton.||||||
68743|Orpheus Supersuite|72668|4|Described|p4, p12, p15-16|||West Pilbara Superterrane. Emplaced into rocks on either side of the SSZ and are contemporaneous with the deposition of the Cleaverville Formation.|c. 3015 Ma|||Intrudes the De Grey Supergroup.|Gabbro,  granite, granodiorite and sills of porphyritic dacite.|
74640|Osmington Seam|22820|5|Briefly described|p10 Fig. 4, p12 Fig. 5, p32|||Of the Rosabrook C.M. This seam is at its thickest and most extensive on the Vasse Shelf - constituting more than 30% of the identified coal resource, thus making it a prime mining target.||||||12-AUG-08
40565|Otorowiri Formation|12758|4|Described|p19, p10 Fig. 10|Early Cretaceous|Early Cretaceous|Supersedes the Otorowiri Member of the former Parmelia Formation. Now of the Parmelia Group. Conformably overlain by Jervoise Formation; conformably overlies the Yarragadee Formation. Geological Province: Vlaming Sub-basin.||||||15-DEC-08
40565|Otorowiri Formation|14227|5|Briefly described|Enclos. 2|Berriasian|Tithonian|Of Parmelia Group. Underlies Carnac Formation. Presented as Otorowiri.||||||07-FEB-11
40565|Otorowiri Formation|24443|5|Briefly described|Fig.31|Early Cretaceous|Late Jurassic|Basal unit of Parmelia Group. Overlies Yarragadee Formation. Conformably overlain by Jervoise Sandstone. Geological Province: Perth Basin.||||||
40565|Otorowiri Formation|50108|5|Briefly described|Map legend|Late Jurassic|Late Jurassic|Of the Parmelia Group. Geological Province: Perth Basin.||||||28-JUL-09
40565|Otorowiri Formation|60376|5|Briefly described|p17 Fig. 4.|Late Jurassic|Late Jurassic|Geological Province: Perth Basin. Of the Parmelia Group. Overlain by Jervoise Sandstone. Underlain unconformably by Yarragadee Formation.||||||02-OCT-15
40565|Otorowiri Formation|60386|5|Briefly described|p318|Berriasian|Berriasian|Perth Basin. Distal shelf/basin.||||||
40565|Otorowiri Formation|61811|5|Briefly described|p3 Fig.2, p65.|Tithonian|Tithonian|Northern Perth Basin. Type section details in Appendix 1.||Unit in Parmelia Group.||Overlies Yarragadee Formation.||
40565|Otorowiri Formation|64580|4|Described|map legend||Late Jurassic|Of Parmelia Group. Micaceous siltstone, shale, minor glauconitic sandstone.||||||15-DEC-08
40565|Otorowiri Formation|64635|5|Briefly described|p4 Fig.3|Tithonian|Tithonian|||Unit in Parmelia Group.||Overlies Yarragadee Formation.||
40565|Otorowiri Formation|67340|6|Mentioned|p6, 8|Early Cretaceous|Jurassic|Northern Perth Basin. See also references to Otorowiri Member (p7-8, 25).||Parmelia Group.||||
40565|Otorowiri Formation|69081|6|Mentioned|p736 Tb.1|||Geol. Prov: Perth Basin||||||
40565|Otorowiri Formation|69182|5|Briefly described|Ch2 p3, Ch2 p9, Ch2 p15|Early Cretaceous|Early Cretaceous|Perth Basin. Misspelt as the Otowowiri Member in Ch2 p15. See also Ch2 p45, Ch2 p52-p53, Ch2 p55, Ch2 p57, Ch2 p60-p63, Ch2 p84-p86.||Parmelia Group||Unconformably overlies the Yarragadee Formation. Overlain by the Parmelia Group.|Fine-grained siltstones and claystones.|
40565|Otorowiri Formation|69297|6|Mentioned|p175, p176, p189|Berriasian|Tithonian|Vlaming Sub-basin, South Perth Basin. ||Parmelia Group||||
40565|Otorowiri Formation|70097|5|Briefly described|p19 Fig.3, p20 Fig.4|Berriasian|Berriasian|Perth Basin. Vlaming Sub-basin, Bunbury Trough and Dandaragan Trough.||Parmelia Group||Overlies Yarragadee Formation. Is overlain by Jervoise Sandstone or Parmelia Group.|Shale, and ?siltstone.|12-SEP-17
40565|Otorowiri Formation|70099|5|Briefly described|Fig.4; p5|Berriasian|Berriasian|Vlaming Sub-basin. Correlated to Mentelle 3 syn-rift Supersequence.||Parmelia Group.||||
40565|Otorowiri Formation|70128|5|Briefly described|p463 Fig.10|Early Cretaceous|Early Cretaceous|Vlaming Sub-basin.||Parmelia Group.||Is overlain by Jervoise Sandstone.||
40565|Otorowiri Formation|70826|6|Mentioned|p7 tbl 4|Early Cretaceous|Jurassic|Perth Basin.||||||
40565|Otorowiri Formation|71377|5|Briefly described|p7|Early Cretaceous|Late Jurassic|Bunbury Trough, Perth Basin.||Parmelia Group||||
40565|Otorowiri Formation|71958|5|Briefly described|p34, p41, p45-p46|Oxfordian|Callovian|Vlaming Sub-basin.||||Overlies the Yarragadee Formation. Overlain by the Jervoise Sandstone.|Silty shales.|
40565|Otorowiri Formation|72034|5|Briefly described|500k_interpgeop16_lut|Berriasian|Late Jurassic|Perth Basin.  Age from biostratigraphy.||Parmelia Group|||Micaceous siltstone, shale, minor glauconitic sandstone.|
75853|Outcamp Bore Tonalite|64775|6|Mentioned|p3-1, 10-1|Neoarchean|Neoarchean||2719 +/- 5 Ma.(SHRIMP zircon: Nelson, 1997).|||||30-MAR-12
28141|Overland Sandstone|14019|3|Fully described|p24-25|Late Cambrian|Late Cambrian|Of the Elder Subgroup. Lithic arkose and sandstone. Conformably overlies Eagle Hawk Sandstone, unconformably underlies the Mahony Group. Type section: 230m. Geological Province: Ord Basin.||||||
28141|Overland Sandstone|40993|6|Mentioned|Fig.1|||||||||
28141|Overland Sandstone|41840|3|Fully described|p43|||Formerly included in the Elder Sandstone.||||||15-DEC-08
28141|Overland Sandstone|41864|4|Described|p26|||||||||
28141|Overland Sandstone|41865|5|Briefly described|Map legend|Late Cambrian|Middle Cambrian|||||||
28141|Overland Sandstone|41866|5|Briefly described|Map legend|Late Cambrian||||||||
28141|Overland Sandstone|43855|5|Briefly described|Map Legend|Boomerangian|Templetonian|||||||
28141|Overland Sandstone|44868|5|Briefly described|Map Legend|Boomerangian|Ordian|||||||
28141|Overland Sandstone|60419|4|Described|p1, 11|Late Cambrian|Late Cambrian|Of Elder Subgroup. Overlies Eagle Hawk Sandstone. Fluvial. Geological Province: Ord Basin.||||||
28141|Overland Sandstone|60519|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Elder Subgroup (Goose Hole Group).  White, fine to medium grained lithic arkose. Geological Province: Ord Basin.||||||03-NOV-04
28141|Overland Sandstone|60589|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Of the Elder Subgroup.  White, fine to medium lithic arkose and sandstone.  Conformably overlies Eagle Hawk Sandstone.  Geological Province: Ord Basin.||||||
28141|Overland Sandstone|64580|6|Mentioned|map legend|||Of Goose Hole Group.||||||15-DEC-08
28141|Overland Sandstone|67860|4|Described|p417 fig4-85, p419 Tb.4-18, p421 fig4-86|Late Cambrian|Late Cambrian|0-230 m thick. Type section details given. Unfossiliferous.||Elder Subgroup||Conformably overlies Eagle Hawk Sandstone.|White lithic feldspathic sandstone; rare shale.|
28141|Overland Sandstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Furongian|Furongian|Ord Basin||Elder Subgroup|||White lithic feldspathic sandstone; rare shale.|04-AUG-15
28141|Overland Sandstone|69165|5|Briefly described|100k_interpgeop_lut.csv|Furongian|Furongian|See also 500k_geologyp08_lut.csv. ||Elder Subgroup|||White lithic feldspathic sandstone, rare shale.|
28141|Overland Sandstone|69437|5|Briefly described|p22:10-11|Series 4|Series 4|Ord Basin, Centralian B Superbasin. Sequence 2. Fluviatile deposits.||||Overlies Eagle Hawk Sandstone.||12-JUL-16
28141|Overland Sandstone|69446|6|Mentioned|p31:4|||Ord Basin.||||||12-JUL-16
28141|Overland Sandstone|69448|3|Fully described|p33:2-4, 6-7|Cambrian|Middle Cambrian|Mory and Beere (1985). Ord Basin. 230m thick at the type section, a steep-sided plateau straddling the WA-NT border in the northwestern LIMBUNYA map area. In WA, the unit thins to the SW and pinches out. Braided fluviatile deposits. Unfossiliferous; most likely late Middle or early Late Cambrian.||Elder Subgroup.||Conformably and gradationally overlies Eagle Hawk Sandstone. Is overlain unconformably by Mahony Group. Correlated with Skewthorpe Formation (Bonaparte Basin).|White to pale grey or fawn, fine to medium lithic arkose and sandstone; trough and planar cross-beds, current ripple marks, parallel lamination.|12-JUL-16
28141|Overland Sandstone|69634|4|Described|GEOL_LUT_CSV files|Furongian|Furongian|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|497-485.4 Ma (Biostrat)|Unit of Elder Subgroup.|||White lithic feldspathic sandstone; rare shale|
28141|Overland Sandstone|69673|5|Briefly described|p194|||230m thick.||Elder Subgroup||Overlies Eagle Hawk Sandstone|Lithic arkose and sandstone.|
28141|Overland Sandstone|70154|5|Briefly described|100k_interpgeop_lut.csv|Ordovician|Cambrian||485-497 Ma|Elder Subgroup|||White lithic feldspathic sandstone; rare shale.|
28141|Overland Sandstone|71267|4|Described|GEOL_LUT_CSV files|Furongian|Furongian|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny (450-295 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|497-485.4 Ma (biostrat)|Unit of Elder Subgroup.|||White lithic feldspathic sandstone; rare shale|
28141|Overland Sandstone|71800|5|Briefly described|p25-p26|Late Cambrian|Middle Cambrian|Ord Basin. Deposited in a fluvial environment.||Elder Subgroup||Overlies the Eagle Hawk Sandstone. Unconformably overlain by the Mahony Group.|White, clayey arkose.|
28141|Overland Sandstone|73255|6|Mentioned|p534 Fig.2|Cambrian|Cambrian|||Goose Hole Group||Overlies the Eagle Hawk Sandstone, disconformably underlies the Buchanan Sandstone.||
83386|Owen Monzogranite|73391|5|Briefly described|p197, 199, 229, 293, 295|||One of two major batholiths in the north Kalgoorlie district. Possibly composite. ~9 km N of Mount Pleasant.|2655 +/- 15 Ma (SHRIMP: Sircombe et al., 2007).||||Light grey, foliated, medium- to coarse-grained, weakly feldspar-porphyritic biotite monzogranite.|
72706|Owens Gully Diorite|64621|5|Briefly described|Map legend|Archean|Archean|Of the Callina Supersuite. Age: 3464-3462Ma. Meta-quartz diorite; foliated to gneissic.||||||07-NOV-08
72706|Owens Gully Diorite|65387|6|Mentioned|p7, p13|Paleoarchean|Paleoarchean|Stern et al. (2007). East Pilbara. This is the current [2008] Pb-Pb monitor in use with SHRIMP analyses at Geoscience Australia. Accepted age, measured 207 Pb / 206 Pb ratio = 0.29907 +/- 0.00011, n=11.|3465 +/- 0.6 Ma, ID-TIMS.|||||
72706|Owens Gully Diorite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Callina Supersuite. Age c.3465-3462 Ma. Meta quartz diorite; foliated to gneissic.||||||29-APR-13
72706|Owens Gully Diorite|66683|6|Mentioned|p369.|||East Pilbara. The OG1 standard used at Geoscience Australia for monitoring SHRIMP instrumental mass fractionation of Pb isotopes. Used with other standards in dating samples for this article.||||||
72706|Owens Gully Diorite|67479|5|Briefly described|p11|Paleoarchean|Paleoarchean|Current Pb-Pb monitor in use at Geoscience Australia.|3464.4 +/- 0.6 Ma|||||24-JAN-17
72706|Owens Gully Diorite|68575|6|Mentioned|p8|||East Pilbara. Used as a Pb-Pb monitor for instrumental mass fractionation during SHRIMP analytical sessions.||||||
72706|Owens Gully Diorite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Callina Supersuite|||Meta quartz diorite; foliated to gneissic|
72706|Owens Gully Diorite|69566|6|Mentioned|p236|||Mount Edgar Granitoid Complex, East Pilbara Granite-Greenstone Terrane.||Callina Supersuite.||||
72706|Owens Gully Diorite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3466-3462 Ma (inferred)|Unit of Callina Supersuite.|||Metamorphosed quartz diorite; foliated to gneissic|
72706|Owens Gully Diorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||quartz diorite|
72706|Owens Gully Diorite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||Max age 3465 +/-1 Ma, min 3462+/-4 Ma.|Callina Supersuite|||Metamorphosed quartz diorite; foliated to gneissic.|
72706|Owens Gully Diorite|72251|6|Mentioned|p62,66-67|Paleoarchean|Paleoarchean|Contains 3.467 Ga zircons, which was assigned to the Mount Edgar Granitic Complex by Kemp et al. (2017).||||||
72706|Owens Gully Diorite|73526|6|Mentioned|p5|Paleoarchean|Paleoarchean||c. 3465.4 Ma|||||
27871|Oxley Chert|24160|6|Mentioned|p27 Tb. 14|Proterozoic|Proterozoic|||Billeranga Subgroup||||
27871|Oxley Chert|24410|6|Mentioned|p142 Tb. 60|||Of the Billeranga Subgroup (Moora Group). ||||||
27871|Oxley Chert|36293|6|Mentioned|p76|||Refers Arriens & Lalor 1959 and Low 1975.||||||
27871|Oxley Chert|36872|4|Described|p74|||||||||
27871|Oxley Chert|37460|6|Mentioned|p178|||||||||
27871|Oxley Chert|40346|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27871|Oxley Chert|40347|6|Mentioned|p19|||||||||
27093|Padbury Group|12099|4|Described|p676-8, 681-4,685-6, Figs.1,2,4, 7,8|Statherian|Orosirian|New or redefined unit by Occhipinti et al. (1997). Age poorly constrained. Lower Padbury Group stratigraphy modified by Martin (1994) who replaced the scheme of Gee (1987) and Windh (1992).|Between 2000 and 1640 Ma.||Includes Millidie Creek, Robinson Range, Wilthorpe and Labouchere Formations.|Unconformably overlain by Bangemall Group. In fault contact with Bryah Group and locally unconformably overlies Bryah Group. In tectonic contact with Narracoota Formation.|Contains quartz wacke, siltstone, conglomerate, iron formation, hematitic shale, and minor clastic rocks and dolomite.|04-MAR-13
27093|Padbury Group|22501|6|Mentioned|p117|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27093|Padbury Group|22694|4|Described|p7|||In Glengarry Basin||||||13-FEB-07
27093|Padbury Group|22695|5|Briefly described|map|Proterozoic|Proterozoic|||||||
27093|Padbury Group|22696|5|Briefly described|map|Proterozoic|Proterozoic|||||||
27093|Padbury Group|22697|5|Briefly described|map|Proterozoic|Proterozoic|||||||
27093|Padbury Group|22698|5|Briefly described|map|Proterozoic|Proterozoic|||||||
27093|Padbury Group|22716|5|Briefly described|table4,p229,234|Paleoproterozoic|Paleoproterozoic|Gascoyne Complex is source of sediment for Padbury Group. Age: 1800Ma.||||||07-NOV-08
27093|Padbury Group|22940|4|Described|p16, Fig.1 p3|Paleoproterozoic|Paleoproterozoic|Probably a retro-arc foreland basin. See also Table 2 p12, Fig.6 p14. of Padbury Basin.||||||07-NOV-08
27093|Padbury Group|23151|5|Briefly described|p64|||||||||
27093|Padbury Group|23156|6|Mentioned|p8|||||||||
27093|Padbury Group|23485|4|Described|p25|Paleoproterozoic|Paleoproterozoic|Geological Province:  Padbury Basin.||||||07-NOV-08
27093|Padbury Group|23487|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Padbury Basin||||||07-NOV-08
27093|Padbury Group|23525|5|Briefly described|p2 Fig. 1||Orosirian|Age: <2000Ma. Geological Province: Padbury Basin||||||
27093|Padbury Group|23586|5|Briefly described|p15|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27093|Padbury Group|23592|4|Described|p12|Paleoproterozoic|Paleoproterozoic|Age: 1996+/-35 Ma (from Wilthorpe Formation). Underlying unit Bryah Group. Geological Province: Padbury Basin.||||||07-NOV-08
27093|Padbury Group|23593|5|Briefly described|p2 Fig 1|||Overlying unit Earaheedy Group. Underlying unit Bryah Group. Geological Province: Padbury Basin.||||||
27093|Padbury Group|23597|6|Mentioned|p8|||||||||
27093|Padbury Group|23600|5|Briefly described|p4 Fig 2|||Geological Province: Padbury Basin.||||||
27093|Padbury Group|23723|5|Briefly described|p1|||Geological Province: Nabberu Basin.||||||
27093|Padbury Group|23744|4|Described|p13|Paleoproterozoic|Paleoproterozoic|Geological Province: Padbury Basin.||||||07-NOV-08
27093|Padbury Group|23747|4|Described|p14|Paleoproterozoic|Paleoproterozoic|Geological Province: Padbury Basin.||||||07-NOV-08
27093|Padbury Group|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Padbury Basin.||||||
27093|Padbury Group|23749|4|Described|p13|Proterozoic|Proterozoic|Geological Province: Padbury Basin||||||
27093|Padbury Group|23750|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Padbury Basin.||||||
27093|Padbury Group|23759|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27093|Padbury Group|23781|5|Briefly described|p27 Fig. 10||Paleoproterozoic|||||||07-NOV-08
27093|Padbury Group|23798|6|Mentioned|p2|||Includes banded iron formation rocks. Geological Province: Yilgarn Craton.||||||05-JUL-06
27093|Padbury Group|23865|6|Mentioned|p170 Fig.1|||Geological Province: Yilgarn Craton.||||||
27093|Padbury Group|23890|5|Briefly described|p21 Fig.11|||Geological Province: Padbury Basin.||||||
27093|Padbury Group|24017|5|Briefly described|p8 Tb. 2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27093|Padbury Group|24021|6|Mentioned|p3, Fig. 1|||||||||
27093|Padbury Group|24028|5|Briefly described|p288 Fig. 1|||||||||
27093|Padbury Group|24183|6|Mentioned|p2 Fig.1|Mesoproterozoic|Mesoproterozoic|||||||
27093|Padbury Group|24332|5|Briefly described|p135 Fig. 1|Paleoproterozoic|Paleoproterozoic|Volcanic and sedimentary rocks. Age: c.2000Ma.||||||07-NOV-08
27093|Padbury Group|24535|6|Mentioned|p23|Paleoproterozoic|Paleoproterozoic|||||||
27093|Padbury Group|24544|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Age: <2000 Ma.||||||07-NOV-08
27093|Padbury Group|29663|2|Defined|p52|Paleoproterozoic|Paleoproterozoic|-||||||07-NOV-08
27093|Padbury Group|30010|4|Described|p45|||||||||
27093|Padbury Group|31217|6|Mentioned|p40|||||||||
27093|Padbury Group|35949|6|Mentioned|Fig.8|||||||||
27093|Padbury Group|35975|1|Redefined|p103|Proterozoic|Proterozoic|||||||
27093|Padbury Group|36551|6|Mentioned|Table 29|||||||||
27093|Padbury Group|37024|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27093|Padbury Group|37213|4|Described|p19|||||||||
27093|Padbury Group|37299|6|Mentioned|Fig.1|||||||||
27093|Padbury Group|37460|6|Mentioned|p144|||||||||
27093|Padbury Group|38298|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27093|Padbury Group|38299|6|Mentioned|p6|||||||||
27093|Padbury Group|39162|5|Briefly described|p51|||||||||
27093|Padbury Group|39427|6|Mentioned|p5|||||||||
27093|Padbury Group|40089|6|Mentioned|p4|||See also P207||||||
27093|Padbury Group|40105|6|Mentioned|Fig.3|||||||||
27093|Padbury Group|40297|6|Mentioned|p109|||||||||
27093|Padbury Group|40935|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27093|Padbury Group|40937|5|Briefly described|p5|||||||||
27093|Padbury Group|40938|6|Mentioned|p4|||||||||
27093|Padbury Group|40989|6|Mentioned|Fig.1|||||||||
27093|Padbury Group|41991|5|Briefly described|p130|||||||||
27093|Padbury Group|42579|5|Briefly described|Table 2, P11|||||||||
27093|Padbury Group|42730|5|Briefly described|Fig 12, P15|||||||||
27093|Padbury Group|43069|5|Briefly described|p19|||see also Fig.2||||||
27093|Padbury Group|43238|4|Described|p6|||||||||
27093|Padbury Group|43561|6|Mentioned|p1436|||||||||
27093|Padbury Group|43595|5|Briefly described|p75,219,343,346||Paleoproterozoic|Deposition age: approx. 1.8-1.7 Ga||||||07-NOV-08
27093|Padbury Group|43831|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
27093|Padbury Group|44867|5|Briefly described|Map Legend||Mesoproterozoic|||||||
27093|Padbury Group|44927|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
27093|Padbury Group|49893|6|Mentioned|p2 Fig.1|||||||||
27093|Padbury Group|49896|1|Redefined|p55 App. 2p2 Tb. 1, p3 Tb. 2|Paleoproterozoic|Paleoproterozoic|Includes Labouchere, Wilthorpe, Robinson Range and Millidie Creek Fms. Siliciclastic succession. Overlies former Glengarry Group (now Yerrida and Bryah Groups), therefore overlies Bryah Group unconformably. Age: 1.9-1.8 Ga. Max. thickness: ~10km.||||||07-NOV-08
27093|Padbury Group|50218|5|Briefly described|p238 Fig. 1, p244|Paleoproterozoic|Paleoproterozoic|Consists of poly-deformed and metamorphosed siliciclastic and chemical sedimentary rocks. Overlies the Bryah Group. Age: <2000Ma. Geological Province: Padbury Basin. See also p242 Fig. 4.||||||07-FEB-11
27093|Padbury Group|50219|5|Briefly described|p258 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: <2000Ma.||||||07-FEB-11
27093|Padbury Group|50221|5|Briefly described|p296 Fig.1, p297|Paleoproterozoic|Paleoproterozoic|Comprises siliclastic, carbonate and chemical sedimentary rocks. Overlies the Bryah Group. Age: <2000 Ma. Geological Province: Padbury Basin.||||||07-NOV-08
27093|Padbury Group|50222|4|Described|p326,  p319 Fig. 2|Paleoproterozoic|Paleoproterozoic|Includes Labouchere, Wilthorpe, Robinson Range and Millidie Creek Fms. Locally unconformably overlies Horseshoe Fm.  In fault contact with Narracoota Fm. and  Yarweelor Gneiss Complex.  Age: <2.0-1.9Ga (Nelson, 1997).  Geol. Prov: Padbury Basin.||||||07-NOV-08
27093|Padbury Group|50225|5|Briefly described|p386 Fig. 1|||||||||07-FEB-11
27093|Padbury Group|50226|6|Mentioned|p421 Fig. 4, p422|||Geological Province: Padbury Basin.||||||
27093|Padbury Group|61217|5|Briefly described|p42 Fig. 1|Proterozoic|Proterozoic|Sedimentary rocks including BIFs.||||||07-FEB-11
27093|Padbury Group|61269|6|Mentioned|p86 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27093|Padbury Group|61271|6|Mentioned|p106, p107|||||||||
27093|Padbury Group|61848|5|Briefly described|p300, p301|||Includes banded iron formations which form prominent ridges.||||||
27093|Padbury Group|62289|5|Briefly described|plate 1, p4 Fig. 2|Palaeoproterozoic|Palaeoproterozoic|Includes Millidie Creek, Robinson Range, Wilthorpe and Labouchere Formations. Geol. Prov: Padbury Basin.||||||29-OCT-15
27093|Padbury Group|63866|5|Briefly described|p162, p164, p168|Paleoproterozoic|Paleoproterozoic|Western Glengarry Basin.|<1900 Ma||Includes the Labouchere, Wilthorpe, Robinson Range and Millidie Creek Formations.|Unconformably overlain by the Collier Group. Overlain by the Edmund Group. Faulted against (and locally unconformably on) the Bryah Group.|Quartz wacke, siltstone, conglomerate, iron-formation, hematitic shale and minor clastic rocks and dolomite.|
27093|Padbury Group|64580|4|Described|map legend||Paleoproterozoic|Metamorphosed sandstone, siltstone, mudstone, banded iron-formation, granular iron-formation, conglomerate, and dolostone.||||||09-DEC-08
27093|Padbury Group|64724|6|Mentioned|p46|||||||Overlies Bryah Group.||02-APR-12
27093|Padbury Group|64725|5|Briefly described|p64.|Paleoproterozoic|Paleoproterozoic|West Australian Craton. Contains amagmatic orogenic, shear zone-hosted, Au lodes.||||||
27093|Padbury Group|64728|6|Mentioned|p94 Fig.1. |Paleoproterozoic|Paleoproterozoic|||||Is unconformably overlain by Bangemall Supergroup.||
27093|Padbury Group|65408|5|Briefly described|pp81 - 85.|Statherian|Orosirian|A peripheral foreland basin succession. Maximum age: Labouchere Formation SHRIMP U/Pb detrital zircon age 2.0-1.9 Ga. Minimum age: Pb/Pb model age: 1.9 - 1.8 Ga of pyrite, galena formed in late stage gold mineralization, Labouchere Formation.|2.0 - 1.9 Ga maximum deposition age, Labouchere Fm||Includes Labouchere, Wilthorpe, Robinson Range and Millidie Formations.|Unconformably overlies Bryah Group.|Clastics; no volcanic component.|21-JAN-22
27093|Padbury Group|65411|4|Described|p88, p89 Fig.1, pp90-91, p94.|Paleoproterozoic|Paleoproterozoic|Lithology is redefined in this article. Padbury Basin. Formerly of Glengarry Basin, a name now abandoned. Is extensively disrupted by faulting, and is tectonically interleaved with lower Bryah Group. Deposition in a foreland basin on the northern margin of the Yilgarn Craton.|||Includes Labouchere, Wilthorpe, Robinson Range and Millidie Creek Formations.|Overlies Bryah Group unconformably. Is faulted against Narracoota Formation.|A sequence of banded iron-formation, hematitic shale, wacke, siltstone conglomerate, and dolomite; also mafic clastic rocks.|
27093|Padbury Group|65412|5|Briefly described|p97 Fig.1.|Paleoproterozoic|Paleoproterozoic||||||Includes turbiditic sediments.|
27093|Padbury Group|65419|1|Redefined|pp1-2, p4 Fig.1, pp36-45.|Paleoproterozoic|Paleoproterozoic|Of Barnett (1975); as redefined by Gee (1979), excluded units below the Wilthorpe Conglomerate; redefinitions by Windh (1992) and Martin (1994, in prep.) reverted to the original definition of Barnett (1975) and included the Labouchere Formation. In Glengarry Basin as defined by Gee and Grey (1993); formerly part of the Nabberu Basin. The name Glengarry Basin is no longer used (Pirajno et al. 1996), hence this unit now occupies the Padbury Basin. Named after Mount Padbury. Type area extends from Mount Padbury area to Mount Fraser and Robinson Range areas. Variable thickness, estimated 5-6 km. Age from Beatty Park Member; the Group is younger than the 2.0 Ga Bryah Group but older than the 1.8 Ga Bangemall Group.|c.2.0 Ga.||Includes Labouchere, Wilthorpe, Robinson Range and Millidie Creek Formations. Included Wilthorpe Conglomerate.|Unconformably overlies the Bryah Group. Is faulted against the Despair Granite. Is unconformably overlain by the Bangemall Group.|Conglomerate, arenite, shale, banded iron-formation and granular iron-formation.|
27093|Padbury Group|65450|5|Briefly described|p1, p2-3, p5 Fig.2, p27|Paleoproterozoic|Paleoproterozoic|Padbury Basin. In former Glengarry Basin, former Glengarry Group. Gold mining.|2.0-1.65 Ga.|||Unconformably overlain by Edmund Group.|Metasedimentary rocks; pelitic, psammitic, and mafic schist.|
27093|Padbury Group|65549|5|Briefly described|Map Legend||Orosirian|Of the Padbury Basin. Informally subdivided into two unnamed metasedimentary units. Age of <2000 Ma given.||||||10-NOV-10
27093|Padbury Group|65896|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Padbury Basin. <2000 Ma. Includes Labouchere, Wilthorpe, Robinson Range, and Millidie Creek Formations.||||||
27093|Padbury Group|65913|6|Mentioned|p2 Fig.1. |||||||||
27093|Padbury Group|66112|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Padbury Basin. Includes Labouchere, Wilthorpe and Robinson Range Formations, as well as a number of mapped but unnamed units, mostly chert, banded iron-formation, siltstones and quartz arenite.||||||
27093|Padbury Group|66427|6|Mentioned|p40 Fig.1|||Deposition in a small foreland basin.||||Overlies Bryah Group.||
27093|Padbury Group|67246|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Padbury Basin.|||Includes Labouchere Formation.|Intruded by Moorarie Supersuite. Is overlain unconformably by Yilgatherra Formation.||
27093|Padbury Group|67346|5|Briefly described|p793, p794 Fig.1, p795 Fig.2|Paleoproterozoic|Paleoproterozoic|Padbury Basin.|||||Metasandstone; metasiltstone, metasandstone and metadolostone; pelitic, psammitic and mafic schist.|11-MAY-12
27093|Padbury Group|67855|4|Described|p206-207,p205,  p209, 221|||Deeply infolded in 3 synclinal keels in Glengarry Fold Belt. Previously correlated with Earaheedy Group, but this now in doubt.|||Wilthorpe Conglomerate, Robinson Range Formation.|Overlies Glengarry Group with angular unconformity.|Conglomerate, shale, BIF and dolomite.|
27093|Padbury Group|67888|6|Mentioned|p54|||Auriferous quartz veins.|||Includes Labouchere Formation|||
27093|Padbury Group|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic|also used in 2_5M_GEOLOGYP98_LUT|||Includes Labouchere Formation, Millidie Creek Formation, Robinson Range Formation, Wilthorpe Formation.|||
27093|Padbury Group|69003|5|Briefly described|p4, p10 Fig.11, p11, p13, p16|||Padbury Basin, Capricorn Orogen.|||Labouchere, Wilthorpe, Robinson Range, Millidie Creek Formations.|||
27093|Padbury Group|69010|5|Briefly described|Map Legend|Statherian|Orosirian|Padbury Basin.|1983-1620 Ma||Includes the Labouchere Formation.|||
27093|Padbury Group|69028|5|Briefly described|Map Legend|Orosirian|Orosirian|Padbury Basin. Where undivided, this group ranges in age between 1983-1811 Ma.|||Includes Millidie Creek Formation, Wilthorpe Formation, and Labouchere Formation.||Undivided: sandstone, siltstone, mudstone, banded iron-formation, granular iron-formation, conglomerate and dolostone.|06-MAY-14
27093|Padbury Group|69080|6|Mentioned|p684|||Yilgarn Craton.|||||Sandstone, siltstone, mudstone, BIF, granular iron-formation, conglomerate and dolostone.|
27093|Padbury Group|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic||||Includes Labouchere Formation, Robinson Range Formation, Wilthorpe Formation, Millidie Creek Formation||Metamorphosed sandstone, siltstone, mudstone, banded iron-formation, granular iron-formation, conglomerate, and dolostone.|
27093|Padbury Group|69387|5|Briefly described|p11|||Narryer Terrane.||||||
27093|Padbury Group|69596|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Capricorn Orogen.||||||
27093|Padbury Group|70795|6|Mentioned|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 2_5m_interpgeop15_lut.csv, West Australian Craton|1983-1811 Ma||||Sandstone, siltstone, mudstone, banded iron-formation, granular iron formation, conglomerate and dolostone.|
27093|Padbury Group|70796|4|Described|2_5m_interpgeop15_lut.csv|Paleoproterozoic|Paleoproterozoic|Of the Padbury Basin, Capricorn Orogen. Minimum age of 1811 +/ 5 Ma (Isotopic). See also 500k_interpgeop14_lut.csv.|ca 1983 +/ 12 Ma (max age; isotopic)||Includes the Millidie Creek Formation, Robinson Range Formation, Wilthorpe Formation and the Labouchere Formation.||Sandstone, siltstone, mudstone, banded ironformation, granular ironformation, conglomerate, and dolostone|
27093|Padbury Group|70804|4|Described|p1-p7, p17-p18, p21-p22|Orosirian|Orosirian|Some units previously assigned to the Glengarry Group have been reassigned to this group. Together with the Bryah Group makes up the western part of the former 'Glengarry Basin'. Ages derived from Nelson (1997) and Windh (1992). Gold and minerals production and remaining resources detailed. See also p24-p34, p37-p38, p42, p44-p45, p47.|c. 2000 Ma-1800 Ma||Includes the Labouchere Formation, Wilthorpe Formation, Robinson Range Formation and the Millidie Creek Formation.|Unconformably overlies the Horseshoe Formation and the Bryah Group.|Quartz wacke, siltstone, conglomerate, iron formations, hematitic shale and minor clastic rocks and dolomite.|
27093|Padbury Group|70814|5|Briefly described|p3, p40, p48-p49|||Padbury Basin.|||Includes the Labouchere Formation.|Unconformably overlain by the Yilgatherra Formation.||
27093|Padbury Group|70826|6|Mentioned|p6 tbl 2, p9|Paleoproterozoic|Paleoproterozoic|Padbury Basin.||||||21-APR-20
27093|Padbury Group|71042|6|Mentioned|p66 fig 2, p98|||||||||24-MAY-19
27093|Padbury Group|71269|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Of Padbury Basin. Events: Capricorn Orogeny (1817-1772 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv.|||Includes Labouchere Formation, Millidie Creek Formation, Robinson Range Formation.||Sandstone, siltstone, mudstone, banded iron-formation, granular iron-formation, conglomerate, and dolostone|
27093|Padbury Group|71468|5|Briefly described|p25,27|Orosirian|Orosirian|Geological province: Capricorn Orogen, Yilgarn Craton. Of Bryah Sub-basin.||||Underlain by Hourseshoe Formation.|Well-bedded metamorphosed quartz-chlorite siltstones.|20-AUG-19
27093|Padbury Group|71484|5|Briefly described|p122-124,125,129,134,136-137,139|||Geological province: Of Padbury Basin. Nomenclature proposed by Hall and Goode 1978 to describe stratigraphy in the western part of the Nabberu Basin (now revised). Can be divided into upper and lower Padbury groups, separated by the Bertibubba Supersuite. Cumulative thickness: 10km. Deposited initiated during Glenburgh Orogeny.|||Includes Moorarie Supersuite, Millidie Creek Foramtion, Robinson Range Formation, Wilthorpe Formation and Labouchere Formation.|||30-AUG-19
27093|Padbury Group|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Padbury Basin.|Max age 1983+/- 12 Ma, Min 1811+/-5 Ma.||Includes Millidie Creek Formation, Robinson Range Formation, Wilthorpe Formation, Labouchere Formation.||Sandstone, siltstone, mudstone, banded iron-formation, granular iron-formation, conglomerate, and dolostone.|
27093|Padbury Group|73102|5|Briefly described|p3|||Yilgarn Craton.|||||Sandstone, siltstone, mudstone, banded iron-formation, granular iron-formation, conglomerate, and dolostone.|
27093|Padbury Group|73442|5|Briefly described|p3|||Yilgarn Craton.|||||Sandstone, siltstone, mudstone, banded iron-formation, granular iron-formation, conglomerate, and dolostone.|
80959|Paleozoic siliciclastic units, Canning Basin 80959|72034|5|Briefly described|500k_interpgeop16_lut|Paleozoic|Paleozoic|Infromal unit. Eastern Canning Basin. Age inferred.|||||Sandstone and siltstone, eastern Canning Basin.|
75245|Palkapiti Formation|66116|5|Briefly described|Map legend|Archean|Archean|Burtville Terrane, Yilgarn Craton. Consists of several units, all metamorphosed. Andesitic volcanic and volcaniclastic rock, dacite, rhyolite, breccia, conglomerate, sandstone, siltstone, mudstone. Two volcanic units have ages of 2770 +/- 3 Ma.||||||
75245|Palkapiti Formation|66117|5|Briefly described|Map legend|Archean|Archean|Merolia Domain, Burtville Terrane, Yilgarn Craton. c.2770 Ma. Comprises numerous units, all metamorphosed, including andesitic volcanic and volcaniclastic rocks, dacites, rhyolites, conglomerate, sandstone, siltstone, shale, chert. ||||||
75245|Palkapiti Formation|66121|5|Briefly described|Map legend|Archean|Archean|Burtville Terrane, Yilgarn Craton. Consists of several units, all metamorphosed. Andesitic volcanic and volcaniclastic rock, dacite, rhyolite, breccia, conglomerate, sandstone, siltstone, mudstone. Sedimentary rocks commonly deeply weathered.||||||
75245|Palkapiti Formation|68107|4|Described|p607 Fig.3, p608 Fig. 4, p609 Tb.1.|Neoarchean|Neoarchean|Mount Venn Greenstone Belt, Burtville Terrane. Geochronology by Wingate et al. (2009), Wingate & Pawley (2009).|2770 +/- 3 Ma; 2769 +/- 3 Ma.|||Intruded by the Mount Venn Igneous Complex and Wartu Monzogranite.|Ranges from andesitic to rhyolitic in composition, and includes coherent flows, tuffaceous rocks, and volcaniclastic breccias and sandstones.|22-SEP-14
75245|Palkapiti Formation|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Merolia Domain, Burtville Terrane, Eastern Goldfields Superterrane, Yilgarn Craton. Metarhyolite in upper part gives Pb/Pb SHRIMP magmatic crystallisation age:  2770+/-3 Ma . Underlying metavolcanic rock in same fm gives igneous crystallisation age of 2769+/-3 Ma. See geochron file 178122.1.pdf (2007), 183118.1.pdf (2009), 193360.1.pdf (2010).|2769+/-3 Ma||Includes 20 unnamed subunits.||Felsic volcanic rocks and siliciclastic sedimentary rocks.|07-AUG-15
75245|Palkapiti Formation|69404|6|Mentioned|p4 Fig.4|Neoarchean|Neoarchean|Burtville Terrane.|c. 2780 Ma|||||
75245|Palkapiti Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|See also 100k_geologyp14_lut.csv and 500k_interpgeop14_lut.csv. Age derived from a metarhyolite sample (178122.1.pdf)|2770 +/- 3 Ma (SHRIMP)||||Felsic schist, andesite, andesitic volcanic and volcaniclastic rock, volcanic sandstone; metamorphosed. Dacite, dacitic-rhyolitic breccia. Rhyolite, rhyolitic sandstone and siltstone. Sandstone, mudstone, siltstone, shale and chert; metamorphosed.|
75245|Palkapiti Formation|70802|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Burtville Terrane, Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events.|2770-2769 Ma (inferred)||||Undivided felsic volcanic and siliclastic sedimentary rocks; metamorphosed|
75245|Palkapiti Formation|71168|6|Mentioned|p10|Neoarchean|Neoarchean|Burtville Terrane, Yilgarn Craton.|2769 +/- 3 Ma to 2770 +/- 3 Ma|||||
75245|Palkapiti Formation|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Burtville Terrane, Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma). Sample GSWA 178122 (metarhyolite) yielded a weighted mean 207Pb/206Pb date of 2770+\-5 Ma, interpreted to be magmatic crystallisation age of the rhyolite. Sample GSWA 183118 (metavolcanic rock) yielded a weighted mean 207Pb/206Pb date of 27769\-3 Ma, interpreted to be igneous crystallisation age of the volcanic rock. See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 100k_geologyp14_lut.csv, 500k_interpgeop_lut.csv, 100k_geologysub14_lut.csv, 2_5m_interpgeop15_lut.csv.|2769+\-2 Ma; 2702-2692 Ma (inferred)||||Felsic volcanics, volcaniclastics, schists from felsic volcanics; andesitic volcanics, volcaniclastics; dacite and dacitic volcaniclastics to rhyolitic breccia; rhyolite, rhyolitic sandstone and siltstone; undivided sedimentary rocks; metamorphosed.|
75245|Palkapiti Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||||||Undivided felsic volcanic and siliclastic sedimentary rocks; metamorphosed.|
75245|Palkapiti Formation|73596|6|Mentioned|p1170|Neoarchean|Neoarchean|Mount Venn Greenstone Belt, Burtville Terrane.|2769 +/- 3 Ma.|||||
77506|Pallas Athena Microgranite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||3010 - 2600 Ma (inferred).||||Plagioclase-biotite microgranite; plagioclase microphenocrysts; massive to strongly foliated; metamorphosed.|
77506|Pallas Athena Microgranite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|3010-2600 Ma (inferred)||||Plagioclase-biotite microgranite; plagioclase microphenocrysts; massive to strongly foliated; metamorphosed|
31890|Pandanus Yard Monzogranite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.||||||07-NOV-08
31890|Pandanus Yard Monzogranite|23751|4|Described|p10|||Cream to pale-grey, medium-grained, weakly porphyritic to evenly textured biotite monzogranite.||||||
31890|Pandanus Yard Monzogranite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1850Ma. Geological province: Kimberley Province (East).||||||07-FEB-11
31890|Pandanus Yard Monzogranite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
31890|Pandanus Yard Monzogranite|43854|5|Briefly described|Map Legend||Proterozoic|Of Paperbark supersuite.||||||
31890|Pandanus Yard Monzogranite|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
31890|Pandanus Yard Monzogranite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31890|Pandanus Yard Monzogranite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite.||||||07-NOV-08
31890|Pandanus Yard Monzogranite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Paperbark Supersuite|||Medium-grained, equigranular or weakly porphyritic biotite monzogranite.|04-AUG-15
31890|Pandanus Yard Monzogranite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Paperbark Supersuite|||medium grained, equigranular or weakly porphyritic biotite monzogranite.|
31890|Pandanus Yard Monzogranite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone|1864-1852 Ma (Inferred)|Unit of Paperbark Supersuite.|||Medium-grained, equigranular or weakly porphyritic biotite monzogranite|
31890|Pandanus Yard Monzogranite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1852-1864 Ma|Paperbark Supersuite|||Medium grained, equigranular to weakly porphyritic biotite monzogranite.|
31890|Pandanus Yard Monzogranite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (183 -1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1864-1852 Ma (inferred)|Unit of Paperbark Supersuite.|||Cream to pale-grey, medium-grained, weakly porphyritic to evenly textured biotite monzogranite.|
79385|Panglo Formation|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma); Yilgarn Craton events (4000 - 2600 Ma).|2657-2640 Ma (inferred)||||Sandstone and conglomerate with minor shale; metamorphosed|
79385|Panglo Formation|73596|6|Mentioned|p1162|||Broad Arrow Inlier, Kalgoorlie Terrane.||||Overlies Black Flag Group.||
80587|Panhandle Dolerite|72712|5|Briefly described|p9, p36, p38, p39, p41, p42,45,48-49,56.|Orosirian|Orosirian|New name equivalent to predominantly NW trending P-d5 dolerite dykes of Tyler (1990, 1991). Not well exposed but extensively studied. Age based on 18 SHRIMP U-Pb analyses of nine samples from a dolerite dyke that cuts the Cheela Springs Basalt at site S72-5 (Fig. 5; Muller et al., 2005). Another site and Paraburdoo mine gave baddeleyite crystallization age of 2009 +/- 16 Ma, based on SHRIMP U-Pb analyses. Further work is required to confirm age. Not known to intrude Wooly Formation.|2007 +/-16 Ma SHRIMP U-Pb baddeleyite|||Intrudes Moodagara Dolerite. Intruded by W-NW trending dykes and by N-NW dykes. Intrudes up to Cheela Springs Basalt.|Dolerite dykes.|14-JAN-21
40198|Panton Suite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Age of Alice Downs Ultrabasics: 1856+/-2 Ma. Data from OZCHRON1. Original comment: 'This is the time of igneous crystallisation of the Panton mafic-ultramafic intrusion (group I intrusion).'|||Includes 6 unnamed units||Metamorphosed layered mafic-ultramafic intrusions. Metadunite, metawehrlite, metalherzolite, metaperidotite; metachromitite layers; metagabbronorite, metagabbro, metanorite; meta-anorthosite.|04-AUG-15
40198|Panton Suite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv. |||||Metadunite, metawehrlite, metalherzolite, metaperidotite, minor metaharzburgite, metagabbronorite, metagabbro, metanorite, metaferrogabbro, metamelagabbro, metaleucogabbro.|
40198|Panton Suite|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Central Zone. See 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|1856-1856 Ma (Inferred)||||Mottled meta-anorthosite, metaleucogabbro, metamelagabbro, metaleucogabbronorite, metamorphosed magnetite gabbro, metanorite, metadunite, metawehrlite, metalherzolite, metaperidotite, minor meta-harzburgite; rhythmic cycles, metachromitite layers|
40198|Panton Suite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv.|1849 Ma||||Metamelagabbro, metaferrogabbro, metagabbronorite, metanorite and metaleucogabbro. Metadunite, metawehrlite, metalherzolite, metaperidotite.|
40198|Panton Suite|70731|6|Mentioned|p269|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. See Panton Intrusion.||||||
40198|Panton Suite|70812|5|Briefly described|p8, p10, p20, p28, p43|Orosirian|Orosirian|Hosts Ni-Cu-Co and PGE-Cr deposits.|c. 1856 Ma||||Mafic-ultramafic layered intrusives.|
40198|Panton Suite|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|||||||
40198|Panton Suite|70851|5|Briefly described|p3-p4, p7, p12, p16-p17|Paleoproterozoic|Paleoproterozoic|Misspelt as Panton Intrusion on p3.|c. 1856 Ma|||Intrudes the Tickalara Metamorphics.||27-MAR-23
40198|Panton Suite|71113|5|Briefly described|p99|Orosirian|Orosirian|Geological province: Central Zone, Lamboo Province, Halls Creek Orogen. Part of a suite of large gabbroic and layered mafic-ultramafic bodies intruding into the Central Zone.|c. 1856 Ma|||||
40198|Panton Suite|71140|6|Mentioned|p99|Orosirian|Orosirian|Central Zone, Lamboo Province, Halls Creek Orogen.|c.1856 Ma.||||Large gabbroic and layered mafic-ultramafic bodies.|
40198|Panton Suite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|1856+\-2 Ma (isotopic)||||Mottled meta-anorthosite, metaleucogabbro, metamelagabbro, metaleucogabbronorite, metamorphosed magnetite gabbro, metanorite, metadunite, metawehrlite, metalherzolite, metaperidotite, minor meta-harzburgite; rhytchmic cycles, metachromitite layers|
40198|Panton Suite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Central Zone, Halls Creek Orogen.|||||Metamorphosed layered mafic--ultramafic intrusions.|
77790|Panton intrusion|60283|4|Described|p24-34|||Within the central zone of the Halls Creek Orogen. 10km long, 2.5km wide, 1.7km thick. Hosts PGM and Au mineralisation. Also presented as Panton Intrusion. Crystallisation age of 1855 Ma. Lithology, structure decribed in detail.||||Intrudes the Tickalara Metamorphics.|Layered differentiated ultramafic-mafic body. Lower 750m is massive serpentinised olivine orthocumulate dunite/peridotite with thin bands of cumulate chromitite-magnetitite. Upper 900m is gabbro and anorthosite.|10-MAY-17
77790|Panton intrusion|60498|5|Briefly described|p1016 Fig.1, p1017.|Paleoproterozoic|Paleoproterozoic|Intrusions form steeply dipping folded sheets, faulted blocks. Cr, PGE, Ni, Cu, Au mineralisation. Strongly differentiated. Chromite deposits have 75 Mt of 1.9 g/t Pt + Pd + Au. Strongly serpentinized due to high ultramafic rocks composition.|1856 +/- 2 Ma (Page & Hoatson 2000).||||Layered mafic-ultramafic intrusion: dunite, harzburgite, chromitite, amphibolite, gabbro, gabbronorite, norite, anorthositic gabbro, anorthosite, ferrogabbro, tremolite-antophyllite peridotite.|03-JAN-18
77790|Panton intrusion|69003|5|Briefly described|p22|Paleoproterozoic|Paleoproterozoic|E Kimberley region, Halls Creek Orogen. Also described as the Panton sill, and the Panton mafic-ultramafic intrusion. Strongly differentiated ultramafic-mafic cumulate intrusion, 10.5 km long and 2.5km wide. Hosts Ni-Cu-PGE in three levels of stratabound chromitite seams or layers.|1856 +/- 2 Ma.||||Comprises a 650m-thick lower ultramafic series (cyclic units of dunite, lherzolite and chromitite) and an upper gabbroic series (gabbro, gabbronorite, norite, ferrogabbro and anorthosite).|
22623|Paperbark Granite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.||||||07-NOV-08
22623|Paperbark Granite|23323|5|Briefly described|p456 Table 1|Orosirian|Orosirian|Age: 1854 +/- 3 Ma.||||||07-FEB-07
22623|Paperbark Granite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1850Ma. Geological province: Kimberley Province (East).||||||07-FEB-11
22623|Paperbark Granite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
22623|Paperbark Granite|43854|5|Briefly described|Map Legend||Proterozoic|Of the Paperbark supersuite.||||||22-NOV-06
22623|Paperbark Granite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
22623|Paperbark Granite|50437|5|Briefly described|p1.5, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite. Age: 1854 +/- 3Ma (Shrimp).||||||07-NOV-08
22623|Paperbark Granite|63866|5|Briefly described|p132|||Western Zone, Halls Creek Orogen.|c. 1854 Ma|Paperbark Supersuite||||
22623|Paperbark Granite|66845|4|Described|p537 Fig.3, p539 Tb.1, p540, p543|||Single analysed zircon grain (no. 46.1) distinctly high Th/U ratio with age 2028 Ma; 16 analyses for magmatic crystallis'n age. The Sally Downs supersuite represents a major episode of granite magmatism that is signicantly younger than the Paperbark supersuite.|magmatic crystallis'n age 1854+/-3 Ma SHRIMP U-Pb|Paperbark supersuite|||Porphyritic monzogranite.|04-AUG-15
22623|Paperbark Granite|66846|5|Briefly described|p558 Table 4|Orosirian|Orosirian|Age probably from U-Pb SHRIMP dating of zircon (see p547). |~1854 Ma|Of Paperbark supersuite.||||
22623|Paperbark Granite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Data from OZCHRON1. Comment: 'This magmatic age for the granite is based on 16 of the 17 analytical data'.|1854+/-3 Ma U/Pb SHRIMP|Paperbark Supersuite|||Medium- to coarse-grained monzogranite and syenogranite with rapakivi texture; medium- to fine-grained biotite-hornblende monzogranite and granodiorite; locally abundant inclusions of mafic rock.|04-AUG-15
22623|Paperbark Granite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv. |1854 Ma|Paperbark Supersuite|||Medium-coarse grained monzogranite and syenogranite with rapakivi texture; medium to fine grained biotite-hornblende monzogranite and granodiorite with local inclusions of mafic rock.|
22623|Paperbark Granite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone.|1854-1854 Ma (Isotopic)|Unit of Paperbark Supersuite.|||Medium- to coarse-grained monzogranite and syenogranite with rapakivi texture; medium- to fine-grained biotite-hornblende monzogranite and granodiorite; locally abundant inclusions of mafic rock|
22623|Paperbark Granite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1854 Ma|Paperbark Supersuite|||Medium to coarse grained monzogranite and syenogranite with rapakivi texture; medium to fine grained biotite-hornblende monzogranite and granodiorite.|
22623|Paperbark Granite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (183 -1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv and geochron files.|1854+\-3 Ma (isotopic)|Unit of Paperbark Supersuite.|||Medium- to coarse-grained monzogranite and syenogranite with rapakivi texture; medium- to fine-grained biotite-hornblende monzogranite and granodiorite; locally abundant inclusions of mafic rock|
22623|Paperbark Granite|72437|5|Briefly described|p81-82, p84-85|||Lamboo Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Foliated biotite-monzogranite, coarse-grained biotite monzogranite and fine-grained biotite monzogranite.|
31788|Paperbark Supersuite|23323|5|Briefly described|p454 Fig.2|Orosirian|Orosirian|Age: 1865-1850 Ma.||||||07-FEB-07
31788|Paperbark Supersuite|23383|5|Briefly described|p6 Fig. 3||Paleoproterozoic|Elsewhere referred to as Paperbark supersuite.  Age 1865-1850 Ma.||||||07-NOV-08
31788|Paperbark Supersuite|23925|5|Briefly described|p222 Table 3|||Geological Province: Halls Creek Orogen.||||||
31788|Paperbark Supersuite|24197|4|Described|p23|||Example of Nicholson Association. Comprises the former Hooper Complex and Bow River Batholith as well as the Whitewater Vols. Relatively homogeneous over wide areas, this was a very large felsic granitic event in the Proterozoic. In Kimberley region.||||||07-FEB-11
31788|Paperbark Supersuite|50437|5|Briefly described|p1.5, 2.1, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Age: 1860-1850Ma. Geological Province: Kimberley Region.||||||07-NOV-08
31788|Paperbark Supersuite|60533|5|Briefly described|p593|Paleoproterozoic|Paleoproterozoic|Age: 1865-1850Ma. Geological Province: Halls Creek Orogen.||||||07-NOV-08
31788|Paperbark Supersuite|62715|5|Briefly described|p1753, p1779|Paleoproterozoic|Paleoproterozoic|Age: 1865-1850Ma.||||||07-NOV-08
31788|Paperbark Supersuite|63866|4|Described|p129, p132-p133, p138|||Western Zone, Halls Creek Orogen. Mistakenly referred to as the Paperback Supersuite on p132. May in part underlie the central Kimberley Basin. Also includes Nyalassy Grnaite, Richenda Microgranodiorite, Bow River Granite, Paperbark Granite and the Kongorow Granite.|||Includes the Lennard Granite, Mondooma Granite, McSherrys Granodiorite, Neville Granodiorite.||Granite plutons with high Rb, Y and low Sr.|
31788|Paperbark Supersuite|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Monzogranite, syenogranite, granodiorite, tonalite; microgranite; micromonzogranite, microgranodiorite, micro-quartz diorite, porphyritic andesite; norite, gabbronorite, gabbro, quartz gabbro, and tonalite; Includes WOMBARELLA QUARTZ GABBRO, TOBY GABBRO.||||||15-DEC-08
31788|Paperbark Supersuite|64730|5|Briefly described|p141|Paleoproterozoic|Paleoproterozoic|I-type. Ages from Tyler et al. 1999; Griffin et al. 2000; Page et al. 2001; Sheppard et al. 2001.|1865-1850 Ma.|||Granites intrude Marboo Formation.||03-MAY-12
31788|Paperbark Supersuite|64731|5|Briefly described|p164|Paleoproterozoic|Paleoproterozoic|Of Bow River Batholith. In Hooper Complex and Western Zone of Hall Creek Orogen.|1860 - 1850 Ma.|||||12-APR-12
31788|Paperbark Supersuite|68078|6|Mentioned|p5, p14 figure 10, p19|Paleoproterozoic|Paleoproterozoic||||Includes Mount Disaster Porphyry, Mondooma Granite|Intrudes Marboo Formation, unconformably overlain by Speewah Group|Granites.|13-SEP-22
31788|Paperbark Supersuite|69003|5|Briefly described|p5, p18-19, p20 Fig.24, p22|||W zone, Lamboo Province. Halls Creek Orogen.|1865-1850 Ma.||Mussel Creek Granite.|Intrudes Marboo Formation.||
31788|Paperbark Supersuite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Includes Springvale Suite; Kongorow, Paperbark, Beefwood Yard, Gordons Gorge, Mount Amy, Mussel Creek, Tumagee, Crooked Creek, Mount Nyulasy, Lennard, Mondooma, Juries Bore Granites; Greenvale, Castlereagh Hill, Mount Disaster Porphyries; Toby Gabbro, Pandanus Yard, Sandy Dam, Survey Creek, Togo Monzogranites; Airfield, Gnewing, Neville Granodiorites; Top Water, Dinner Creek Tonalites; Whitewater Volcanics; and 7 unnamed units.|||||Granite, microgranite, metagranite, monzogranite, pegmatite, norite, gabbro, gabbronorite, layered mafic-ultramafic intrusions, and felsic volcanic rock; net-vein complexes; extensive mingling, and limited mixing, of mafic and felsic magmas|04-AUG-15
31788|Paperbark Supersuite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Also includes Gordons Gorge Granite, Mussel Creek Granite, Pandanus Yard Monzogranite, Sandy Dam Monzogranite, Survey Creek Monzogranite, Togo Monzogranite, Tumagee Granite, Springvale Suite, Crooked Creek Granodiorite, Crooked Creek Granite. See also 500k_interpgeop_lut.csv.|||Includes Paperbark Granite, Beefwood Yard Granite, Greenvale Porphyry, Toby Gabbro||Granite, microgranite, gabbro, layered mafic-ultramafic intrusions, felsic volcanic rock, foliated, biotite bearing rapakivi metagranite. Biotite monzogranite, biotite bearing norite and gabbronorite.|
31788|Paperbark Supersuite|69422|5|Briefly described|p7:3|Orosirian|Orosirian|Considered to be comagmatic with the Whitewater Volcanics.|1865-1850 Ma.||Bow River Granite.||Includes monzogranite, syenogranite and granodiorite; lesser tonalite.|12-JUL-16
31788|Paperbark Supersuite|69585|5|Briefly described|p1-2, p4, p7, p27, p31-32|Orosirian|Orosirian|Erosion of this unit during the Halls Creek Orogeny supplied sediment for the Speewah Group.|1865-1850 Ma.|||Intrudes Marboo Formation. Is overlain nonconformably by O'Donnell Formation (Speewah Group).|Felsic and subordinate mafic and ultramafic magmatic rocks.|
31788|Paperbark Supersuite|69597|6|Mentioned|p3, p5, p68|Paleoproterozoic|Paleoproterozoic|Lamboo Province. |1865-1850 Ma||Includes the Whitewater Volcanics.|Intrudes the Marboo Formation.||
31788|Paperbark Supersuite|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Also includes PORPHYRY: Castlereagh Hill, Greenvale, Mount Disaster; TONALITE: Dinner Creek, Top Water; GRANODIORITE: Gnewing, Neville; MONZOGRANITE: Pandanus Yard, Sandy Dam, Survey Creek, Togo; GABBRO: Toby; Whitewater Volcanics. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 250k_geologyp_lut.csv, 500k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 100k_interpgeol_lut.csv, 250k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv.|1864-1852 Ma (Isotopic)||Includes: GRANITE: Beefwood Yard, Crooked Hill, Gordons Gorge, Juries Bore, Kongorow, Mondooma, Mount Amy, Mount Nyulasy, Mussel Creek, Paperbark, Tumagee.||I-type porphyritic biotite monzogranite and granodiorite; biotite-bearing norite, gabbronorite and minor gabbro; veins of intermediate hybrid rock; hybrid rock cut by veins of coarse-grained porphyritic tonalite and granodiorite.|
31788|Paperbark Supersuite|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Kimberley Craton. Various facies are un-named but mapped separately: aplitic dykes, pegmatite, quartz-feldspar porphyritic microgranite dykes, and isolated dykes of amphibolite. |||Includes Whitewater Volcanics; Mount Disaster Porphyry; Mondooma, Lennard, Mount Amy, Kongorow Granites.||Undifferentiated: granite, microgranite, gabbro, layered mafic-ultramafic intrusions, and felsic volcanic rock.|
31788|Paperbark Supersuite|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province; Halls Creek Orogen; North Australian Craton.|||Whitewater Volcanics; Mount Disaster, Bickleys Porphyries; Mondooma, Lennard Granites; Richenda Microgranodiorite; Scrutons, Baker (misspelling of Barker) Monzogranites.||Granite, microgranite, layered mafic-ultramafic intrusions, and felsic volcanic rock (section only).|
31788|Paperbark Supersuite|70154|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also contains Richenda Microgranodiorite, Scrutons Monzogranite, Whitewater Volcanics, Top water Tonalite, Paperbark Granite, Beefwood Yard Granite, Greenvale Porphyry, Toby Gabbro, Barker Monzogranite, Gordons Gorge Granite, Mussel Creek Granite, Pandanus Yard Monzogranite, Sandy Dam Monzogranite, Springvale Suite. See also 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv.|||Barker Monzogranite, Bickleys Porphyry, Lennard Granite, Mount Disaster Porphyry, Mondooma Granite||Porphyritic rhyolite to andesite; coarse phenocrysts of K-feldspar, quartz and plagioclase. Granite, microgranite, gabbro, layered mafic-ultramafic intrusions and felsic volcanic rock. Rapakivi metagranite, biotite monzogranite.|
31788|Paperbark Supersuite|70731|5|Briefly described|p267-268,272,274,276,278|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. Likely formed in a post-collisional setting (Griffin et al., 2000).  In contact with c. 1855 Ma Corridor Gabbro, characterised by back-veining and pillow-lava textures at contact zone, indicating mafic intrusion into still-cooling felsic rocks. Emplacement of c. 1857 Ma Springvale and c. 1855 Toby layered mafic intrusions at 8-18km depth during Hooper Orogeny.||||Overlain locally by Whitewater Volcanics.||
31788|Paperbark Supersuite|70812|4|Described|p3, p6-p8, p10|Orosirian|Orosirian|Cogenetic with the Whitewater Volcanics. Mineralisation is described, it is noted there are no documented mines or deposits within this suite. See also  p19-p20, p22, p28, p30, p36.|1865-1850 Ma|||Overlain by the Speewah Group. Intrudes the Marboo Formation.|Granites and gabbros.|
31788|Paperbark Supersuite|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|Kimberley.|||||Granites.|
31788|Paperbark Supersuite|70851|5|Briefly described|p3-p4, p12, p16-p20, p24, p29-p30, p35|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province. Geochemistry suggests this unit formed in a post collisional setting.|c. 1865-1850 Ma||Includes the Whitewater Volcanics and the Corridor Gabbro?|||27-MAR-23
31788|Paperbark Supersuite|71113|5|Briefly described|p96,99|Orosirian|Orosirian|Geological province: Western Zone, Lamboo Province, Halls Creek Orogen. Gabbros intruded into Marboo Formation at 1865-1850 Ma. Geochemical characterictics suggest formation in a post-collisional setting (Griffin et al., 2000).|c. 1865-1850 Ma|||||
31788|Paperbark Supersuite|71140|6|Mentioned|p96, 99-100|Orosirian|Orosirian|Western Zone, Lamboo Province, Halls Creek Orogen.|1865-1850 Ma.|||Intrudes Marboo Formation.|Includes gabbros.|
31788|Paperbark Supersuite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (183 -1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). Also includes Richenda Microgranodiorite; GRANITES: Beefwood Yard, Chaneys, Crooked Creek, Dyasons, Gorgon Gorge, Juries Bore, Kongorow, Lennard, Lerida, Long Hole, Matchbox, Mondooma, Mount Amy, Mount Nyulasy, Mulkerins, Mussel Creek, Paperbark, Tumagee; PORPHYRIES: Bickleys, Castlereagh Hill, Greenvale, Mount Disaster; TONALITES: Dinner Creek, Nellie, Top Water; GABBROS: Toby, Wombarella Quartz; Whitewater Volcanics; MICROGRANITES: Square Top, Tarraji. See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyp_lut.csv, 1m_interpgeop_lut.csv, 100k_interpgeol_lut.csv, 250k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv and geochron files.|1864+\-4 to 1852+\-4 Ma (isotopic)||Includes GRANODIORITES: Airfield, Black Rock, Gnewing, McSherrys, Neville; MONZOGRANITES: Barker, Cascade Bay, Louisa, Neil Creek, Pandanus Yard, Sandy Dam, Scruttons, Survey Creek, Togo.||I-type porphyritic biotite monzogranite and granodiorite; biotite-bearing norite, gabbronorite and minor gabbro; veins of intermediate hybrid rock; hybrid rock cut by veins of coarse-grained porphyritic tonalite and granodiorite.|
31788|Paperbark Supersuite|71281|4|Described|p421-423, p431-432|Paleoproterozoic|Paleoproterozoic|Lamboo Province. Generated at the peak of the 1870-1850 Ma Hooper Orogeny.|1864-1852 Ma.||Whitewater Volcanics.|Intrudes Marboo Formation. Is overlain unconformably by O'Donnell Formation (Speewah Group).|Felsic plutonic and volcanic rocks.|
31788|Paperbark Supersuite|71397|4|Described|p1-2,5,47|Orosirian|Orosirian|Geological province: Western Zone, Lamboo Province, Halls Creek Orogen. Griffin et al. (2000a) and Sheppard et al. (1999b) proposed that the Paperbark Supersuite lay inboard of an intervening oceanic arc (Central Zone) at the time of turbidite deposition in the Eastern Zone.|1864-1852 Ma||Includes Whitewater Volcanics.|Intrudes into Marboo Formation and Ruins Dolerite.|Plutonic rocks include medium- to coarse-grained high-K, I-type granites dominated by monzogranite with granodiorite, syenogranite and lesser tonalite, biotite-bearing norite, gabbronorite, gabbro and diorite.|
31788|Paperbark Supersuite|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen, North Australian Craton.|1867 - 1849 Ma.||Lerida, Chaneys, Lennard, Tumagee, Mulkerins, Long Hole Granites; Mount Disaster, Bickleys Porphyries; Top Water Tonalite; Whitewater Volcanics; Neville Granodiorite; Little Gold River Microgranite.||Granite, microgranite, gabbro, layered mafic-ultramafic intrusions, and felsic volcanic rock.|
31788|Paperbark Supersuite|71873|5|Briefly described|p426-427,442-444|Orosirian|Orosirian|Geological province: Lamboo Province. Coeval with c. 1863-1850 Ma Hooper Orogeny. Coincides with Rose Bore Granite and Panton Intrusion and Ruins Dolerite, which reflects the suturing of the Western and Central zones during the amphibolite-granulite facies Hooper Orogeny|1864-1852 Ma||Includes Whitewater Volcanics.|Intruded into Ruins Dolerite and Marboo Formation.||
31788|Paperbark Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Central Zone, Halls Creek Orogen.|Max age 1864+/-4 Ma, Min 1852+/-4 Ma.||Includes Whitewater Volcanics.||Granite, microgranite, gabbro, layered mafic--ultramafic intrusions, and felsic volcanic rock.|
31788|Paperbark Supersuite|72437|5|Briefly described|p4-p5, p9-11, p59, p90, p111|||Co-magmatic with the Whitewater Volcanics. Equates to the Bow River batholith of Sheppard et al., 1995. 700 km-long belt. Intrudes the Hooper Complex and the western Lamboo Complex. Subdivided into 41 named granitoid and gabbro plutons Whole-rock analyses and REE analyses are provided. Also includes Long Hole Granite, Louisa Monzogranite, Black Rock Granodiorite, Pillara Monzogranite, Gnewing Granodiorite, Mad Gap Monzogranite, Tumagee Granite, Mussel Creek Granite, Airfield Granodiorite, Top Water Tonalite, Paperbark Granite, Sandy Dam Monzogranite, Togo Monzogranite, Pandanus Monzogranite, Survey Creek Monzogranite, Kevins Dam Monzogranite, Mount Nyulasy Granite, Dinner Creek Tonalite, Crooked Creek Granite, Neil Creek Granite, Gordons Gorge Granite, Matchbox Granite, Wombarella Quartz Gabbro, Toby gabbro, Kongorow Granite, Nellie Tonalite, Secure Bay Monzogranite, Barker Monzogranite.|||Includes Lerida Granite, Scrutons Monzogranite, Dyasons Granite, McSherrys Granodiorite, Chaneys Granite, Lennard Granite, Mulkerrins Granite.||Granitoids and coeval massive gabbro.|
31788|Paperbark Supersuite|72490|6|Mentioned|p3-5|Orosirian|Orosirian|Lamboo Province.|1864-1852 Ma|||Intrudes Marboo Formation.|Granitic rocks.|
31788|Paperbark Supersuite|73089|6|Mentioned|p35-36|Orosirian|Orosirian|Lamboo Province, far western. Zircon Hf isotope values have been obtained for four 1867-1865 Ma granitic rocks [see text].|1867-1849 Ma||||Felsic Igneous Rocks.|
79349|Papertalk Granite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|3010-2600 Ma (inferred)||||Strongly foliated metagranite and granitic schist|
77234|Papulankutja Supersuite|67375|5|Briefly described|p6, pp8-9 Fig.5, p12 Fig.8, pp17-21. |Mesoproterozoic|Mesoproterozoic|Isolated remnants of ancient crust, outcropping between the communities of Blackstone and Jameson.|1402 +/- 4 Ma (Kirkland et al. in prep.).||||Granodiorites and monzogranites.|
77234|Papulankutja Supersuite|67553|5|Briefly described|p9,11,14,16,19,22-23|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province, North Australian Craton. Restricted to Tjuni Purlka Tectonic Zone. Age based on SHRIMP U-Pb geochronology. Calc-alkaline magmatism at 1402+\-14 Ma (GSWA 194764).|c. 1400 Ma|||||
77234|Papulankutja Supersuite|68077|5|Briefly described|p3-5, p7-10, p14-16, p18, p24, p27-34|Mesoproterozoic|Mesoproterozoic|See also p36-37, p42-43. Limited emplacement S of Mount Scott, Tjuni Purlka Tectonic Zone. Rocks are compositionally indistinguishable from those of the younger Wankanki Supersuite. Represents the oldest known magmatic rocks in the west Musgrave. Isotopic composition (Lu-Hf and Sm-Nd) and evolution tabulated and discussed in detail.|1402 +/- 4 Ma.||||Calcic to calc-alkaline granodiorites and monzogranites, granite.|07-SEP-17
77234|Papulankutja Supersuite|68995|5|Briefly described|p2|Ectasian|Calymmian||c. 1400 Ma||||Intrusive (and possibly extrusive) calc-alkaline magmas.|
77234|Papulankutja Supersuite|69003|5|Briefly described|p4, p37-39|Mesoproterozoic|Mesoproterozoic|Oldest rocks in the west Musgrave Province, Paterson Orogen.|c.1400 Ma.||||Felsic gneisses.|
77234|Papulankutja Supersuite|69091|4|Described|p54 Fig.4.2, p56, see comments|Mesoproterozoic|Mesoproterozoic|Of west Musgrave Province. Papulankutja Supersuite metagranites are geochemically similar to Wankanki Supersuite (1345-1293 Ma Mount West Orogeny), however their ages differ. See also p58 Fig.4.5, p60-1, p183, p186 (incl Fig.9.8).|1402 +/- 4 Ma, zircons, Kirkland et al. 2011|||Is cut by dyke of Wankanki Supersuite.|Felsic magmatism; sample of a moderately foliated, K-feldspar porphyritic, orthopyroxene-clinopyroxene-biotite granodiorite to monzogranite, metamorphosed at or near granulite-facies conditions; calcalkaline suite.|
77234|Papulankutja Supersuite|69153|6|Mentioned|GEOCHRON/194764.1.pdf||Mesoproterozoic|Age mentioned in GEOCHRON/194764.1.pdf|c.1400 Ma (Howard et al.,2011)|||||
77234|Papulankutja Supersuite|69436|5|Briefly described|p21:5|Mesoproterozoic|Mesoproterozoic|Detrital zircon ages (appearing as 1.4-1.3 Ma)[!].|1.4 - 1.3 Ga (Wade et al. 2008).|||||12-JUL-16
77234|Papulankutja Supersuite|69554|6|Mentioned|p139|||Western Musgrave Province.|||||Orthogneisses.|
77234|Papulankutja Supersuite|69655|5|Briefly described|p4|Mesoproterozoic|Mesoproterozoic|West Musgrave Province.|||||Felsic-calc alkaline granitic magmas.|
77234|Papulankutja Supersuite|69729|5|Briefly described|p70-71, p88|Mesoproterozoic|Mesoproterozoic|Southern Tjuni Purlka Zone. Amongst the oldest exposed rocks in west Musgrave Province. Minimum age (of the foliation) is c.1318 Ma from an unfoliated dyke.|c.1402 Ma (U-Pb zircon crystallisation age).||||Metagranites: moderately foliated, K-feldspar porphyritic, orthopyroxene-clinopyroxene-biotite granodioritic and monzogranitic granulite.|
77234|Papulankutja Supersuite|70083|6|Mentioned|p206|||Western Fregon Subdomain, Musgrave Inlier.|c.1400 Ma.||||Felsic calc-alkaline intrusives.|
77234|Papulankutja Supersuite|70084|4|Described|p219-221,223-225,227|Calymmian|Calymmian|Geological province: Musgrave Province, Paterson Orogen. Correlable to Loogana Arc in the Madura Province. Contains c. 1402 Ma protolith ages (Kirkland et al., 2013a). Lies within a single, narrow, Nd and Hf-isotopic evolution band with TDM2 values within a range of 2.2-1.6 Ga, together with the Pitjantjatjara, Wankanki and Warlawurru supersuites, reflecting reworking of juvenile crust between ca. 2.0 and 1.6 Ga (Kirkland et al., 2013a).|c. 1400 Ma|||||09-JUN-20
77234|Papulankutja Supersuite|70634|6|Mentioned|194764.1.pdf|Mesoproterozoic|Mesoproterozoic|SHRIMP age derived from a foliated monzogranite sample (194764.1.pdf)|1402 Ma +/- 4 Ma(SHRIMP)||||Calc-alkaline granitics.|
77234|Papulankutja Supersuite|70793|5|Briefly described|194764.1.pdf|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province. Represents outcrop of a previously unrecognised igneous basement that is significantly older than Wankanki Supersuite (Smithies et al., 2010). Sample GSWA 194764 (foliated monzogranite) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) magmatic crystallisation age of 1402+\-4 Ma, and a 207Pb*/206Pb* metamorphic rim growth date of 1316+\-8 Ma. Sample GSWA 194767 (psammitic enclave in gneiss) yielded an interpreted (weighted mean 207Pb*/206Pb*) maximum depositional age of 1404+\-15 Ma for the protolith of the psammitic enclave, and a high-grade metamorphic age (weighted mean 207Pb*/206Pb*) of 1313+\-5 Ma, and prolonged metamorphic zircon growth (207Pb*/206Pb*) from 1205-1154 Ma. Sample GSWA 194768 (migmatitic paragneiss) yielded an interpreted (weighted mean 207Pb*/206Pb*) maximum depositional age of 1390+\-15 Ma for the sedimentary protolith, high grade metamorphism and migmatisation date (weighted mean 207Pb*/206Pb*) of 1311+\-21 Ma, and prolonged metamorphic zircon growth at 1206-1167 Ma (207Pb*/206Pb*).||||||
77234|Papulankutja Supersuite|70826|6|Mentioned|p10|Mesoproterozoic|Mesoproterozoic|Mount West Orogeny.|1345-1293 Ma (Age of Orogeny)|||||
77234|Papulankutja Supersuite|70831|5|Briefly described|p2, p25|Ectasian|Calymmian|West Musgrave Province.|c. 1400 Ma|||Intruded by the Wankanki Supersuite.|Metagranitic rocks including paragneiss.|
77234|Papulankutja Supersuite|70839|5|Briefly described|p326-327,339|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province. Felsic calc-alkaline intrusive (and possibly extrusive) magmatism.|c. 1.4 Ga|||||
77234|Papulankutja Supersuite|71088|5|Briefly described|p4, p25|||West Musgrave Province.|c. 1400 Ma||||Felsic calc-alkaline magmatic rocks.|
77234|Papulankutja Supersuite|71170|5|Briefly described|p8, p44|Mesoproterozoic|Mesoproterozoic|West Musgrave Province. May represent the early magmatism during initial subduction associated with the amalgamation of the South-Australian and North-Australian Craton.|c. 1400 Ma ||||Felsic calc-alkaline magmatic rocks.|
77234|Papulankutja Supersuite|71210|6|Mentioned|p5-p6|||Musgrave Province.|c. 1400 Ma|||||
77234|Papulankutja Supersuite|71211|5|Briefly described|p228|Calymmian|Calymmian|West Musgrave Province. |ca. 1410 Ma||||Granites.|
77234|Papulankutja Supersuite|71268|5|Briefly described|194764.1.pdf|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province. Represents outcrop of a previously unrecognized igneous basement significantly older than the 1345-1293 Ma Wankanki Supersuite in the Mount Scott area (Smithies et al., 2010). Sample GSWA 194764 (foliated monzogranite) yielded weighted mean 207Pb/206Pb dates of 1402+\-4 and 1316+\-8 Ma, interpreted as the magmatic crystallization age of the monzogranite, and age of high-grade metamorphism. Sample GSWA 194767 (psammitic enclave in gneiss) yielded a weighted mean 207Pb/206Pb date of 1404+\-15 Ma, interpreted as the maximum depositional age of the sedimentary protolith, and high-grade metamorphism, migmatisation and zircon recrystallisation at 1313+\-5 Ma. Sample GSWA 194768 (migmatitic paragneiss) yielded weighted mean 207Pb/206Pb dates of 1390+\-15 Ma and 1311+\-21, interpreted as the magmatic crystallization age of the monzogranite, and high-grade metamorphism, migmatisation and zircon recrystallisation respectively.|c. 1400 Ma|||||
77234|Papulankutja Supersuite|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1402+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Monzogranite.|
77234|Papulankutja Supersuite|72094|5|Briefly described|p2|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Second oldest known rocks of the west Musgrave Province. Underwent UHT metamorphism during Musgrave Orogeny.|c. 1400 Ma||||Granitic rocks.|
77234|Papulankutja Supersuite|72242|5|Briefly described|p27|Ectasian|Calymmian|Geological province: Musgrave Province. Post-dates Coorabie Orogeny, coeval with Loongana Arc bimodal magmatism.||||||
77234|Papulankutja Supersuite|73058|5|Briefly described|p760-761, p769-771, p777 Fig.14, p779|Ectasian|Calymian|Musgrave Province. Typically felsic, metaluminous, calcic to calc-alkaline. Felsic orthogneiss with a protolith age of 1402+/-4 Ma assigned to the Papulankutja Supersuite, emplaced into sediment and crosscut by 1318+/-9 Ma unfoliated dyke constrains age of deformation. Zircon ages of 1313+/-15 Ma, 1298+/-26 Ma and 1311+/-21 Ma interpreted as migmatisation during Mount West Orogeny. Hf and Nd model ages suggest mantle extraction event at c. 1900 Ma. Location in text includes p772 Fig.8-9, p773-774, p778.|c. 1400 Ma||||Typically granodiorites and monzogranites, foliated; gneisses include felsic orthogneiss.|
77234|Papulankutja Supersuite|73166|6|Mentioned|p652 Fig. 8, p656|Mesoproterozoic|Mesoproterozoic|Musgrave Province.|ca 1400 Ma|||||
77234|Papulankutja Supersuite|73225|5|Briefly described|p19|||Western Musgrave Province. Composition is consistent with an arc setting.|c.1402 Ma.|||||
77234|Papulankutja Supersuite|73345|6|Mentioned|p228|||||||||
29988|Paraburdoo Member|22689|6|Mentioned|138|Paleoproterozoic|Archean|Of Wittenoom Formation,  Hamersley Basin Age 2505 +- 37 Ma||||||07-NOV-08
29988|Paraburdoo Member|22701|4|Described|p37|Siderian|Archean|Also Fig2,p39. Wittenoom Formation, Hamersley Basin. 2505 +/- 37 Ma. Overlies Marra Mamba Iron Formation. Overlain by Bee Gorge Member.||||||07-NOV-08
29988|Paraburdoo Member|23612|5|Briefly described|p843|||Of Wittenoom Formation.||||||
29988|Paraburdoo Member|23890|5|Briefly described|p9|Paleoproterozoic|Archean|Of Wittenoom Formation, Hamersley Group. Geological Province: Hamersley Basin.||||||07-NOV-08
29988|Paraburdoo Member|24544|4|Described|p57 Fig.43|Archean|Archean|Of Wittenoom Formation. Overlies West Angela Member. Overlain by Bee Gorge Member. Dolomite. Geological Province: Hamersley Basin.||||||07-NOV-08
29988|Paraburdoo Member|43064|3|Fully described|p68|||Of Wittenoom Formation. Reserved as Paraburdoo.||||||07-APR-09
29988|Paraburdoo Member|43290|5|Briefly described|p6||Archean|of Wittenoom Formation(Simonson et al;1993)||||||07-NOV-08
29988|Paraburdoo Member|60373|6|Mentioned|p145 Tb. 1|Archean|Archean|Of Wittenoom Formation.||||||23-JUN-09
29988|Paraburdoo Member|60706|5|Briefly described|p623 Fig.2|||Of the Wittenoom Formation. Geological Province: Hamersley Basin.||||||11-APR-05
29988|Paraburdoo Member|61575|5|Briefly described|p759|||Of the Wittenoom Formation. ||||||
29988|Paraburdoo Member|61576|5|Briefly described|p773|||Of the Wittenoom Formation. Composed mostly of dolomite with minor chert and argillite partings. Overlain by Bee Gorge Member.  Geological Province: Hamersley Basin.||||||
29988|Paraburdoo Member|62129|3|Fully described|p9|Archaean|Archaean|Of Wittenoom Formation. Thickness: 450m. Geological Province: Hamersley Basin. Thin- to thick-bedded dolomite with minor amounts of chert and argillite and tabular bedding.||||||07-FEB-11
29988|Paraburdoo Member|67130|5|Briefly described|p3 fig 2|||||Wittenoom Formation||Overlies West Angela Member, overlain by Bee Gorge Member|Carbonates.|
29988|Paraburdoo Member|67201|6|Mentioned|p34 Fig.18|||||Wittenoom Formation||||24-NOV-16
29988|Paraburdoo Member|67721|5|Briefly described|p38 Fig.9|Neoarchean|Neoarchean|Approximately 480 m thick.|c. 2553 Ma|Of the Wittenoom Formation.|||Dolomite/magnesian limestone.|
29988|Paraburdoo Member|68035|4|Described|p292 Fig 6|Neoarchean|Neoarchean|Hamersley Group, Hamersley Basin.||Of Wittenoom Formation.||Overlies West Angela Member, overlain by Bee Groge Member|Carbonate.|
29988|Paraburdoo Member|68280|6|Mentioned|p5|||||Wittenoom Formation|||Carbonates.|17-JAN-23
29988|Paraburdoo Member|69538|5|Briefly described|p517 Fig.3, p528-530, p571-572|||See also p574-576, p583-585. Includes part of what the authors call the Fortescue Reef limestone.||Unit in Wittenoom Formation.|||Includes carbonates. Manganiferous-goethitic crusts common.|
29988|Paraburdoo Member|69563|5|Briefly described|p691|||Contains a spherule marker bed aged c.2.57 Ma.||Unit in Wittenoom Formation.||||
29988|Paraburdoo Member|69745|6|Mentioned|p272, 277|||Crops out poorly in the Mount Wall Fe deposit area, Hamersley Province. Appears as Paraburdoo Formation on p277.||Wittenoom Formation (lower part).|||Shales, dolomite.|
29988|Paraburdoo Member|71808|4|Described|vii, p2, p22-p23, p32, p37, p44|||Hamersley Province. Poorly exposed monotonous sequence; however, the upper 50m is very well exposed on the face of The Governor and south side of Mount Robinson. A moderately good exposure is present at the west end of South Alligator. 110 m to over 420m thick however the present mapping suggests a thickness between 350 to 500m. Distinguishing characteristics are discussed in greater detail. Deposited as a periplatformal derived pelagic carbonate ooze or mud. See also p54, p56, p59, p102, p107, p117, p127, p177, p239.||Wittenoom Formation|||Well bedded, grey, hemipelagic, crystalline, deep water dolomitised carbonate and associated chert beds.|
29988|Paraburdoo Member|72447|6|Mentioned|p240-241|||||Wittenoom Formation||||
29988|Paraburdoo Member|72493|5|Briefly described|p30|||Hamersley Basin.||Wittenoom Formation.||Overlies West Angelas Member. Is overlain by Bee Gorge Member.|Carbonates.|
29988|Paraburdoo Member|72569|4|Described|p1-2, p16-22|||Of the Hamersley Basin. Assumed to be 260m thick at the type section near Paraburdoo. Lumpy laminations in this unit are attributed to microbial mat fossils. Depositional model for this unit is discussed in detail. Alternating mud and sand beds are explained by progressive increasing and decreasing bottom current velocities.|2590-2570 Ma (interp age)|Wittenoom Formation||Overlies West Angela Shale Member, is overlain by Bee Gorge Member.|Extensive package of carbonate sedimentary rock comprising dominantly dolomite with minor argillite and chert partings.|
29988|Paraburdoo Member|73022|6|Mentioned|p2, p3 Fig.2, p4 Fig.3, p6 Fig.8, p7|||||Wittenoom Formation||Overlies the West Angela Member, underlies the Bee Gorge Member.|Carbonate sediment.|
29988|Paraburdoo Member|73290|6|Mentioned|p784|||Hamersley Province.||||||
29988|Paraburdoo Member|73538|6|Mentioned|p4|||||Wittenoom Formation||Underlain by West Angela Member. Overlain by Bee Gorge Member.|Carbonates.|
79399|Paradise Formation|71000|6|Mentioned|p65, 79-80, 83|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, southern Gascoyne Province, Capricorn Orogen. Hosts the Glenburgh Au deposit; mineralisation occurred between c.2035 and 1991 Ma in a fore-arc or accretionary wedge setting.|c.2035-1997 Ma (deposition).||||Metasedimentary rocks.|
80069|Paradise Well diatexite|69596|6|Mentioned|p5|Orosirian|Rhyacian|Gascoyne Province.||||||
26095|Parda Formation|7433|5|Briefly described|p25 Fig.2,  p42, p45. |Cretaceous|Cretaceous|Canning Basin. Lagoonal or shallow marine fine clastics. 30 m thick sequence.||||Disconformably overlies Melligo Sandstone, Callawa Formation and Broome Sandstone. Is disconformably overlain by Frezier Sandstone in central part of the basin.|Thin-bedded to massive mudstone and fine sandstone.|
26095|Parda Formation|22717|5|Briefly described|P11, P13|Cretaceous|Jurassic|||||||
26095|Parda Formation|22738|4|Described|9,13,14,16,17, map|Early Cretaceous|Early Cretaceous|Max thickness 10 m. Overlying unit Frezier Sandstone, underlying units Broome Sandstone, Callawa Formation||||||
26095|Parda Formation|22765|5|Briefly described|P11, Table1||Aptian|Underlying unit is the Melligo Sandstone||||||
26095|Parda Formation|23415|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Geological province: Westralian Superbasin. White, thin-bedded, and massive mudstone and claystone, and minor lenses of fine-grained sandstone; macrofossils.  Shallow marine deposits.||||||07-JAN-08
26095|Parda Formation|23575|5|Briefly described|Map Legend|Mesozoic|Mesozoic|||||||
26095|Parda Formation|23583|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Underlying unit Callawa Formation. Geological Province Westralian Super Basin.||||||
26095|Parda Formation|23585|4|Described|p25|Cretaceous|Cretaceous|Geological Province: Westralian Superbasin.||||||
26095|Parda Formation|23757|4|Described|p17|Cretaceous|Cretaceous|Disconformably overlies Callawa Formation. Thickness: ~120m. Geological Province: Westralian Superbasin. Shallow-marine, thin-bedded to massive white mudst. + claystone, with some fine-gr. sst and siltst. lenses; ammonite sp. found. See also p7 Fig. 3.||||||01-OCT-08
26095|Parda Formation|24025|5|Briefly described|p16|Cretaceous|Cretaceous|Geological Province: Carnarvon Basin.||||||
26095|Parda Formation|24110|5|Briefly described|Plate 1|Cretaceous|Cretaceous|Geological Province: Northern Carnarvon and Canning Basins||||||
26095|Parda Formation|32648|6|Mentioned|p32|||L.Cret.||||||
26095|Parda Formation|32979|6|Mentioned|p38|||Correlation with basins in India.||||||
26095|Parda Formation|33165|6|Mentioned|p57|||Refers Veevers & Wells (1961)||||||
26095|Parda Formation|34363|6|Mentioned|p56|||Neocomian. See Fig.7.||||||
26095|Parda Formation|36257|6|Mentioned|Table 2.1|||||||||
26095|Parda Formation|36890|3|Fully described|p352|||||||||
26095|Parda Formation|37368|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
26095|Parda Formation|37370|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
26095|Parda Formation|37564|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
26095|Parda Formation|38878|6|Mentioned|Map legend|Aptian|Neocomian|Neocomian - Aptian.||||||
26095|Parda Formation|39857|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
26095|Parda Formation|40078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
26095|Parda Formation|44143|4|Described|p.431 Table 4-19|Cretaceous|Cretaceous|Up to 30m thick; mudstone with fine sandstone lenses; lagoonal or shallow marine. Disconformably overlies Melligo and Broome Sandstones, and Callawa Formation; is overlain disconformably by Frezier Sandstone. Contains rare unidentified bivalves. Type section at Parda Hill (LAGRANGE: 18deg 56' 10" S, 121deg 59' 20" E).||||||24-NOV-17
26095|Parda Formation|44357|4|Described|p14,Tb.1 p8|||Probably Aptian age.||||||
26095|Parda Formation|44443|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|||||||
26095|Parda Formation|44479|2|Defined|Tb.1|||E/51-1. Correlates undiff. Mesozoic of this Sheet.||||||
26095|Parda Formation|44998|2|Defined|p162-164||Early Cretaceous|Overlies Broome Sandstone. Underlies Frezier Sandstone. Lower Cretaceous. See also p119-121,128,133,148,154,183-8,199, map.||||||
26095|Parda Formation|45153|2|Defined|App.8-136|Aptian|Aptian|Defined by: Lindner & Drew (in McWhae & others, 1958, p. 107}. Type section: Parda Hill, south of Broome (18degrees56 'S, 121degrees59 'E; 230 in Table 6). Lithology: In the type area consists of interbedded siltstone and fine-grained sandstone (McWhae & others, 1958). In Parda No. 1 it comprises claystone, grading to finely micaceous, argillaceous siltstone. The sediments have been lateritised.||||||14-DEC-22
26095|Parda Formation|45158|3|Fully described|p12|||See also p35.||||||10-FEB-20
26095|Parda Formation|46319|4|Described|p18|Aptian|Aptian|Originally named Anketell Formation. Overlain by Callawa Formation.  Geological Province: Canning Basin.||||||14-DEC-22
26095|Parda Formation|50544|5|Briefly described|p64-65, p16 Tb. 1,  p62|Cretaceous|Cretaceous|Overlies Paterson Formation; disconformably overlies Callawa Fm.  Age: 120.5-98.9Ma, although correlation with the Windalia Radiolarite ammonites suggests Late Aptian.  Max. thickness: >20m.  Geological Province: Canning and Northern Carnarvon Basins.||||||
26095|Parda Formation|50555|5|Briefly described|Map legend|Cretaceous|Cretaceous|White, thin-bedded, massive mudstone and claystone, with minor lenses of fine-grained sandstone; microfossils.  Geological Province: Canning and Northern Carnarvon Basins (Westralian Superbasin).||||||
26095|Parda Formation|64449|5|Briefly described|p62 Tb. 2|Early Cretaceous|Early Cretaceous|Consists of siltstones and minor fine-grained sandstones.||||||07-FEB-11
26095|Parda Formation|64580|4|Described|map legend||Early Cretaceous|Mudstone; interbedded fine-grained sandstone.||||||09-DEC-08
26095|Parda Formation|64643|5|Briefly described|p3 Fig. 2|Early Cretaceous|Early Cretaceous|||||||10-FEB-20
26095|Parda Formation|65301|5|Briefly described|p5 Fig. 4|Early Cretaceous|Early Cretaceous|Geological province: Canning Basin.||||||
26095|Parda Formation|65449|6|Mentioned|p6|Early Cretaceous|Early Cretaceous|||||Overlies Broome Sandstone. Is overlain by Anketell Formation.||
26095|Parda Formation|67202|5|Briefly described|p44 Fig.2.10, p69-71, p126, p128, p135|Early Cretaceous|Early Cretaceous|Canning Basin. Up to 30m thick. Lagoonal or shallow-marine beach deposits. Conductivity images.||||Overlies Callawa Formation. Is overlain by Frezier Sandstone.|Thin-bedded and massive mudstone and fine sandstone.|
26095|Parda Formation|68007|6|Mentioned|p4|Early Cretaceous|Early Cretaceous|Canning Basin.||||||25-FEB-20
26095|Parda Formation|68902|6|Mentioned|p9 fig 5|Cretaceous|Cretaceous|||||Overlies Broome Sandstone, overlain by Anketell Formation.||
26095|Parda Formation|69167|4|Described|geologyp_lut.csv|Early Cretaceous|Early Cretaceous||||||Mudstone; interbedded fine-grained sandstone.|10-FEB-20
26095|Parda Formation|69182|6|Mentioned|Ch4 p9, Ch4 p45, Ch4 p47|Early Cretaceous|Early Cretaceous|Canning Basin. ||||Overlies the Broome Sandstone. Overlain by the Anketell Formation.||10-FEB-20
26095|Parda Formation|69185|4|Described|GEOL_LUT_CSV files||Early Cretaceous|Of Northern Carnarvon and Canning basins. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|||||Mudstone; interbedded fine-grained sandstone|
26095|Parda Formation|69297|6|Mentioned|p337, p352|Aptian|Aptian|Broome Platform of the Canning Basin. ||||Overlies the Melligo Sandstone. Overlain by the Frezier Sandstone.||
26095|Parda Formation|69590|4|Described|GEOL_LUT_CSV files|Early Cretaceous|Early Cretaceous|Of Wallal Embayment, Ankatell Shelf, Canning Basin. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|145-101 Ma (inferred)||||Mudstone; interbedded fine-grained sandstone|
26095|Parda Formation|70774|5|Briefly described|p4|Early Cretaceous|Early Cretaceous|Canning Basin.||||Overlies the Broome Sandstone. Overlain by the Anketell Formation.||10-FEB-20
26095|Parda Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||claystone, sandstone, mudstone|
26095|Parda Formation|71894|5|Briefly described|p4|Early Cretaceous|Early Cretaceous|Canning Basin.||||Overlies the Broome Sandstone. Overlain by the Anketell Formation.|Sandstone.|10-FEB-20
26095|Parda Formation|72034|5|Briefly described|500k_interpgeop16_lut|Early Cretaceous|Early Cretaceous|Anketell Shelf; Pardoo Shelf; Wallal Embayment, Canning Basin; Roebuck Basin.|||||Mudstone; interbedded fine-grained sandstone.|
26095|Parda Formation|72499|5|Briefly described|p7 Fig.6.|Early Cretaceous|Early Cretaceous|Located in the Broome Platform.||||Overlies Broome Sandstone. Underlies Anketell Formation. Laterally equivalent to Frezier and Melligo Sandstones.|Includes sandstone.|
26095|Parda Formation|73117|5|Briefly described|p3|Lower Cretaceous|Lower Cretaceous|Canning Basin.||||Underlain by Broome Sandstone. Overlain by Anketell Formation. Equivalent to Samuel Formation, Frezier Sandstone, and Melligo Sandstone.|Dominantly sandstone.|
26833|Paringa Basalt|22534|6|Mentioned|Fig.5 p10|||of Kalgoorlie Group||||||
26833|Paringa Basalt|22666|5|Briefly described|p696, Fig.1b|||||||||
26833|Paringa Basalt|23057|5|Briefly described|446|||||||||
26833|Paringa Basalt|23137|4|Described|p245 Table.2|||Of the Kalgoorlie Group.||||||14-APR-08
26833|Paringa Basalt|23139|4|Described|p234 Fig.2, p235|||||||||
26833|Paringa Basalt|23786|5|Briefly described|p10|Archean|Archean|Of Kambalda Group. Geological Province: Yilgarn Craton.||||||07-NOV-08
26833|Paringa Basalt|23795|6|Mentioned|p12|||Geological Province: Yilgarn Craton.||||||
26833|Paringa Basalt|23924|5|Briefly described|p205|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
26833|Paringa Basalt|23926|5|Briefly described|p17|||||||||
26833|Paringa Basalt|23928|5|Briefly described|p64|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
26833|Paringa Basalt|24091|6|Mentioned|p44|||Geological Province: Yilgarn Craton.||||||
26833|Paringa Basalt|24169|5|Briefly described|p668|Archean|Archean|Geological Province : Yilgarn Craton.||||||07-NOV-08
26833|Paringa Basalt|24196|5|Briefly described|p47 Fig.5|||Unconformably overlain by the Spargoville Formation. Overlies the Kapai Slate. Geological Province: Kalgoorlie Terrane.||||||28-MAY-04
26833|Paringa Basalt|24322|5|Briefly described|p61 Fig. 2|Neoarchean|Neoarchean|Age: 2690 +/- 5Ma.  Of the Kambalda Group.||||||07-NOV-08
26833|Paringa Basalt|24325|5|Briefly described|p61 Fig. 2|Archean|Archean|Of the Kambalda Group. Overlies the Kapai Slate. Age: 2690 +/- 5 Ma. Geological Province: Kambalda Dome, Yilgarn Craton.||||||07-NOV-08
26833|Paringa Basalt|29418|6|Mentioned|p116|||||||||
26833|Paringa Basalt|29681|5|Briefly described|Table 2|||||||||
26833|Paringa Basalt|29784|6|Mentioned|Table 1|||||||||
26833|Paringa Basalt|30779|6|Mentioned|Table 1|||Stratigraphy||||||
26833|Paringa Basalt|30882|6|Mentioned|p50|||||||||
26833|Paringa Basalt|30886|6|Mentioned|Table 2|||See also Table 4.||||||
26833|Paringa Basalt|30900|6|Mentioned|p67|||On Table 1||||||
26833|Paringa Basalt|31042|6|Mentioned|Fig. 4|||Correlation||||||
26833|Paringa Basalt|32685|5|Briefly described|Table 1|||||||||
26833|Paringa Basalt|33513|4|Described|p29|||See also p27. Main ore host.||||||14-APR-08
26833|Paringa Basalt|33514|6|Mentioned|p19|||||||||
26833|Paringa Basalt|33515|6|Mentioned|p33|||||||||
26833|Paringa Basalt|33535|4|Described|p177|||||||||
26833|Paringa Basalt|33554|6|Mentioned|p72|||||||||
26833|Paringa Basalt|33917|6|Mentioned|p177|||||||||
26833|Paringa Basalt|34324|6|Mentioned|p112|||||||||
26833|Paringa Basalt|34608|6|Mentioned|p2|||||||||
26833|Paringa Basalt|35611|6|Mentioned|Fig.2|||Stratigraphic columns for Kalgoorlie and Kambalda.||||||
26833|Paringa Basalt|35612|6|Mentioned|p4|||Discussed re Kalgoorlie gold deposits||||||
26833|Paringa Basalt|36259|5|Briefly described|p63|||Underlies Golden Mile Dolerite.||||||12-MAR-08
26833|Paringa Basalt|36869|6|Mentioned|p48|||||||||
26833|Paringa Basalt|38765|6|Mentioned|p100|||||||||
26833|Paringa Basalt|39046|6|Mentioned|p439|||||||||
26833|Paringa Basalt|39895|5|Briefly described|p55|||||||||
26833|Paringa Basalt|40005|5|Briefly described|p13|||||||||
26833|Paringa Basalt|40083|6|Mentioned|p118|||||||||
26833|Paringa Basalt|40845|4|Described|p81|||||||||
26833|Paringa Basalt|40849|6|Mentioned|p37|||||||||
26833|Paringa Basalt|41066|5|Briefly described|p32|||||||||
26833|Paringa Basalt|41149|6|Mentioned|p1665|||||||||
26833|Paringa Basalt|41249|6|Mentioned|p4|||||||||
26833|Paringa Basalt|41368|6|Mentioned|Fig.1|||||||||
26833|Paringa Basalt|41379|6|Mentioned|p42|||||||||
26833|Paringa Basalt|41458|6|Mentioned|p361|||||||||
26833|Paringa Basalt|41588|4|Described|p245|||||||||
26833|Paringa Basalt|41644|6|Mentioned|p219|||||||||
26833|Paringa Basalt|41771|6|Mentioned|Fig.3|||||||||
26833|Paringa Basalt|41784|6|Mentioned|p65|||||||||
26833|Paringa Basalt|41889|6|Mentioned|p218|||||||||
26833|Paringa Basalt|41890|5|Briefly described|p278|||Short form of Paringa Basalt Formation||||||
26833|Paringa Basalt|42117|5|Briefly described|Table 1 P67|||||||||
26833|Paringa Basalt|42160|6|Mentioned|p46|||||||||
26833|Paringa Basalt|42195|5|Briefly described|p146|||See also Fig.4||||||
26833|Paringa Basalt|42221|6|Mentioned|Table 1 P6|||||||||
26833|Paringa Basalt|42344|6|Mentioned|p52|||||||||
26833|Paringa Basalt|42406|5|Briefly described|Fig.2 P250|||||||||
26833|Paringa Basalt|42696|6|Mentioned|Plate 1B|Archean||||||||07-NOV-08
26833|Paringa Basalt|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
26833|Paringa Basalt|42817|5|Briefly described|Fig.3|||||||||
26833|Paringa Basalt|42870|5|Briefly described|Table 1, P67|||||||||
26833|Paringa Basalt|42892|6|Mentioned|Table 3|||||||||
26833|Paringa Basalt|42969|6|Mentioned|Fig.1 p106|||||||||
26833|Paringa Basalt|43102|5|Briefly described|p8|||||||||
26833|Paringa Basalt|43162|6|Mentioned|5|||||||||
26833|Paringa Basalt|43496|5|Briefly described|12|||||||||03-MAR-10
26833|Paringa Basalt|44149|6|Mentioned|p88 Fig.2-90, p91 Tb.2-9|Archean|Archean|Kalgoorlie area, Eastern Goldfields Province.||||||
26833|Paringa Basalt|45546|14|Not recorded|p.50,52|||||||||
26833|Paringa Basalt|46905|5|Briefly described|Table 1|||Stratigraphic succession||||||
26833|Paringa Basalt|50556|5|Briefly described|p1116 Fig.6||Archean|Eastern Goldfields Province.||||||07-NOV-08
26833|Paringa Basalt|50622|4|Described|p314|||High Mg. Overlying unit is Black Flag Beds.||||||
26833|Paringa Basalt|60076|5|Briefly described|p12 Tb. 2|||Mostly high-Mg basalt.  Max. thickness: 800m.  Geological Province: Kambalda domain.||||||
26833|Paringa Basalt|60514|4|Described|p29, p41 Fig. 11, p54, p65 Tb. 1|Archean|Archean|Includes; Defiance Dolerite + Williamstown Dolerite. Overlain conformably by Black Flag Group, underlain by Kapai Slate. Age: 2690+/-5 Ma from interflow chert, high in the Paringa Basalt. Max thickness: 1500m. Consists of pillowed flows + dolerite units. Geol Prov: Kambalda Domain, Yilgarn Craton.||||||13-JUN-13
26833|Paringa Basalt|60555|6|Mentioned|p5, p6 Fig. 3|Archean|Archean|Underlain by Kambalda Komatiite and Kapai Slate, overlain by Black Flag Group.||||||07-NOV-08
26833|Paringa Basalt|60578|6|Mentioned|p6 Fig.1|Archean|Archean|||||||07-NOV-08
26833|Paringa Basalt|60623|4|Described|p25 Fig. 2|Archean|Archean|Age: 2690+/-5 Ma. Of Kalgoorlie Group. Conformably overlies Kapai Slate. Unconformably overlain by Black Flag Gp. Contains thin variolitc, pillowed basalt flows and thick, differentiated dolerite units. Thickness: 500-1500m. Geo. Prov.: Eastern Goldfields||||||12-JUN-15
26833|Paringa Basalt|60626|5|Briefly described|p54|||Thickness: 400-700 m. Basal high Mg flows with variolitc and spinifex textures, and upper pillow and flow breccia textures, with less Mg and more Fe. ||||||
26833|Paringa Basalt|60627|5|Briefly described|p65 Tb.1|||Of Kalgoorlie Group.||||||
26833|Paringa Basalt|62108|5|Briefly described|p1409 Tb. 3|Archean|Archean|Of Kalgoorlie Gp. Siliceous, high Mg basalt, variolitic and pillowed, with numerous chert interflows. Overlies Williamstown Dolerite. Age: 2690+/-5Ma. Max.thick: 1500m. Geol Prov: Yilgarn Craton. See also p1417 Fig. 10,  p1420 Fig. 14.||||||07-FEB-11
26833|Paringa Basalt|62109|5|Briefly described|p1428, p1436|||Pillowed to massive magnesian lavas. Geological Province: Norseman-Wiluna fold belt/Yilgarn Craton. See also p1429 Fig. 2.||||||14-APR-08
26833|Paringa Basalt|62110|5|Briefly described|p1442 Fig. 1|Archean|Archean|Age: 2690+/-5Ma. Geological Province: Kambalda dome in the Norseman-Wiluna greenstone belt, Yilgarn Carton.||||||07-FEB-11
26833|Paringa Basalt|62111|5|Briefly described|p1458 Fig. 2|||Of the Kambalda Group. High-MgO pillowed and massive metabasalt. Geological Province: Kambalda Dome in the Norseman-Wiluna greenstone belt of the Yilgarn Craton.||||||07-FEB-11
26833|Paringa Basalt|62406|5|Briefly described|p55|||Pillowed lava, containing continuous beds of carbonaceous shale and the well-known Green Leader Oroya Shoot sandwiched between sediment and layered felsitic porphyry (or tuff).||||||
26833|Paringa Basalt|62872|5|Briefly described|p806|||||||||
26833|Paringa Basalt|63163|5|Briefly described|p76|||Underlies Golden Mile Dolerite. Max. thickness: 750m - grading from high Mg basalts at base to gradually more evolved tholeiitic basalts towards the top. Geological Province: Kalgoorlie Terrane/Eastern Goldfields Province.||||||04-APR-07
26833|Paringa Basalt|63637|6|Mentioned|p9|||This unit has undeformed contact with the Black Flag Group.  Geological province: Eastern Goldfields Province.||||||17-OCT-07
26833|Paringa Basalt|63981|6|Mentioned|p93 Fig.3, p100|Archean|Archean|NW Kambalda Domain. Kambalda Sequence.|||||Tholeiitic and high MgO basalt.|
26833|Paringa Basalt|64340|5|Briefly described|p7|||Together with Devon Consols Basalt and Kapai Slate, overlies the Kambalda Komatiite.||||||11-OCT-12
26833|Paringa Basalt|64633|6|Mentioned|p4 Fig.3, p6 Fig.4.|||Kalgoorlie Terrane.||Unit in Kambalda Sequence.||||
26833|Paringa Basalt|64715|5|Briefly described|p3, p4, p5 Fig. 4|||Komatiitic basalt. See also p6, p7 Fig. 7, p10.||||||16-DEC-08
26833|Paringa Basalt|65204|6|Mentioned|pg6 Tbl.1|Archean|Archean|Komatiitic and tholeiitic basalt.||||||11-JUN-15
26833|Paringa Basalt|65834|6|Mentioned|p7, 44-48, 53-58, 62|||Kambalda Domain, Kalgoorlie Terrane.||Kalgoorlie Group.||||
26833|Paringa Basalt|66880|6|Mentioned|p7. |Archean|Archean|||Topmost unit in Kambalda Sequence.||Overlies Kapai Slate. Is unconformably overlain by Spargoville Formation.||
26833|Paringa Basalt|67020|6|Mentioned|p660.|Archean|Archean|||||Overlies Kapai Slate. Is overlain by Black Flag Group.||
26833|Paringa Basalt|67198|4|Described|p5 Fig.2, p81, p83, p88-89, p118-119|Neoarchean|Neoarchean|See also p122, p125, p132-133. Kalgoorlie Terrane. Exceeds 500m in thickness. Geochemically subdived into slightly LREE enriched komatiitic basalt to high magnesium tholeiitic basalt and a slightly LREE depleted basalt. Geochemistry is discussed further in detail. Has xenocrystic zircons with >3.4 Ga cores.|2690 +/- 5 Ma|Kambalda Sequence||Overlies Kapai Slate and Devon Consols Basalt, overlain by Spargoville Formation. Is intruded by Kambalda Granodiorite.|Massive or pillowed mafic flows; often pillowed dolerite/gabbro intrusions.|11-SEP-17
26833|Paringa Basalt|68110|6|Mentioned|p685|||Appears also as Paringa Basalts on p685.||||||
26833|Paringa Basalt|68216|6|Mentioned|p301 Fig. 1|||SH51-9||||||09-OCT-12
26833|Paringa Basalt|68217|4|Described|71-73, 75-6|Precambrian|Precambrian|Gold mineralisation. approx. 1000 - 3000 feet thick [~300-900 m thick]||||Underlain by Williamstown Dolerite. Overlain by Golden Mile Dolerite.|Meta-basaltic lavas, in part pillow lavas, with minor interbedded slates.|04-OCT-12
26833|Paringa Basalt|68289|5|Briefly described|p6-p7, p11-p14, p29, p31|||Southern Kalgoorlie Terrane. Part of the mafic-ultramafic succession which is overlain by the Black Flag Group. >500m thick. Outcrop localities are provided.||||Overlies the Kapai Slate. Overlain by the Black Flag Group. Intruded by the Kambalda Granodiorite and Defiance Dolerite.|Deeply weathered pillowed basalt with variolitic textures and breccias.|
26833|Paringa Basalt|69035|5|Briefly described|p412, pp414-418, p420|Neoarchean|Neoarchean||2610 +/- 30 Ma, Rb-Sr (Turek 1966)|||||
26833|Paringa Basalt|69583|5|Briefly described|p37|||Southern Kalgoorlie Terrane. Over 500m thick.||||Is overlain unconformably by Black Flag Group.||
26833|Paringa Basalt|69619|6|Mentioned|p115|||||||Overlies Devon Consols Basalt.||
26833|Paringa Basalt|69631|5|Briefly described|p7, p11, p14-16, p25, p28|||Kambalda area, Kalgoorlie Terrane. Over 500m thick.||||Overlies Kapai Slate. Is overlain by Black Flag Group.|Metamorphosed pyroxene-spinifex-textured basalt characterised by skeletal and acicular amphibole that pseudomorphs primary clinopyroxene, and minor biotite in a matrix of fine-grained amphibole, chlorite, clinozoisite, albite and quartz.|
26833|Paringa Basalt|70020|4|Described|p121|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton. ||Unit of Kambalda Sequence.||Overlain by Spargoville Formation/Kalgoorlie Sequence. Underlain by Kapai Slate.|Basalt, dolerite/gabbro intrusions.|
26833|Paringa Basalt|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2692 - 2680 Ma (inferred).|Hannans Subgroup|||Basalt; massive, pillowed or with pyroxene-spinifex textures; minor thin, fine-grained sedimentary units; metamorphosed. Mafic schist, metashale, metasandstone and metasiltstone as thin units within basaltic flows.|
26833|Paringa Basalt|70287|6|Mentioned|p188, 190-192|||Kalgoorlie Gold Field, Eastern Goldfields Province, Yilgarn Craton.||||Overlies Kapai Slate. Is overlain unconformably by Black Flag Beds.||
26833|Paringa Basalt|70290|6|Mentioned|p296-299|||Kalgoorlie district, Yilgarn Craton. Trace element composition tabulated.||||Overlies Williamstown gabbro.|Tholeiitic pillow basalt. Greenschist facies metamorphism.|
26833|Paringa Basalt|70326|5|Briefly described|p360-362|Neoarchean|Neoarchean|Geological province: Kambalda Domain, Kalgoorlie Terrane, Yilgarn Craton. LREE-enriched basalts (Clout, 1991).|c. 2690 Ma (Claut, 1991)|||Overlain by Black Flag Group. Underlain by Kapai Slate, Kambalda Komatiite and Lunnon Basalt.||
26833|Paringa Basalt|70773|5|Briefly described|iv, p18 fig 11, p21, p23|Neoarchean|Neoarchean|Kambalda Domain, Kalgoorlie Terrane. See also p24 fig 16, p25 fig 18, p26.|c. 2694 Ma|Kambalda Sequence||Overlies the Devon Consols Basalt. Overlain by the Spargoville Formation.|Pillowed or massive basalt, gabbro and dolerite.|
26833|Paringa Basalt|70863|6|Mentioned|p9|||Kambalda Dome, Yilgarn Craton.||||||
26833|Paringa Basalt|71148|6|Mentioned|p122, 130-131, 135|Neoarchean|Neoarchean|Kalgoorlie Terrane, Eastern Goldfields Superterrane, Yilgarn Craton. Presented also as Paringa basalt. Geochemistry detailed.|2692 +/- 4 Ma.|Kambalda Sequence.||||
26833|Paringa Basalt|71166|5|Briefly described|p118, p119 fig 3.89|||Hosts gold mineralization in the Fimiston Superpit. ||||Overlain by the Black Flag Group.||
26833|Paringa Basalt|71168|5|Briefly described|p9|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton.||||Overlies the Kapai Slate. Overlain by the Spargoville Formation.||
26833|Paringa Basalt|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).  See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2692-2680 Ma (inferred)|Unit of Hannans Subgroup.|||Basalt; massive, pillowed or with pyroxene-spinifex textures; minor thin, fine-grained sandstone and siltstone; metamorphosed; mafic schist.|
26833|Paringa Basalt|71308|4|Described|p710-711, p714, p725-726, p728-p729|||Southern Kalgoorlie Terrane. Said to be the "type" stratigraphic unit for the authors' High-Th Siliceous Basalts group. Geochemistry, petrogenesis discussed in detail. Type area is between Kalgoorlie and Kambalda. Also appears as Paringa basalt (eg p726).|2700-2690 Ma.|Kambalda Sequence.|||Pillows and massive flows; commonly shows characteristic variolitic and pyroxene micro-spinifex textures, and glomerophyric olivine.|12-DEC-18
26833|Paringa Basalt|71309|5|Briefly described|p737, p740, p742, p748-749, p758|||Kalgoorlie Terrane. Enriched: geochemistry and petrogenesis discussed in detail.||||||
26833|Paringa Basalt|71803|6|Mentioned|p369, p378|||Kalgoorlie Terrane, Yilgarn Craton.|ca. 2680 Ma|||||
26833|Paringa Basalt|72049|6|Mentioned|p258-p260, p267-p268|||Spatially close relationship with the doleritic units which intrude the Kambalda Sequence; immobile-element geochemistry is very similar too.||Kambalda Sequence||Overlies the Kapai Slate.|Mafic and basaltic rocks.|
26833|Paringa Basalt|72057|6|Mentioned|p244|Neoarchean|Neoarchean|Geological province: Yilgarn Craton.||||||
26833|Paringa Basalt|72095|4|Described|p4, p6-17,20-21|Neoarchean|Neoarchean|Eastern Goldfields, Yilgarn Craton. Basement to the Kalgoorlie-Kambalda region. Extensively intruded by mafic and ultramafic sills. Contains High-Th Siliceous Basalt (HTSB) geochemistry. Detailed geochemistry is described.||Unit of Hannans Subgroup.||Overlies Kapai Slate. Overlain by Black Flag Group.||
26833|Paringa Basalt|72252|5|Briefly described|p11-15, 18-19, 22-24|||St. Ives Au-Ni camp, Kambalda Domain, Yilgarn Craton. 500 - 1000m thick. Hosts the rich Hamlet underground Au mine. Chemically fractionated.|||||Siliceous high-Mg basalt, with submarine pillowed and massive facies; thick differentiated dolerite units; minor interflow sediments. Metamorphosed to greenschist facies.|
26833|Paringa Basalt|72485|6|Mentioned|p3 Fig.2|||||Kambalda Sequence.||||
26833|Paringa Basalt|72568|6|Mentioned|p4, p13|||Uppermost unit in the Kambalda Sequence. Cut by mafic dykes that are contemporaneous with the CAL. Appears as Paringa Basalts on p13.|2720 - 2680 Ma|||||
26833|Paringa Basalt|73238|6|Mentioned|p4|||Eastern Goldfields Terrane.||||||
26833|Paringa Basalt|73300|6|Mentioned|p1112-1113, p1118 Fig.7|||Yilgarn Craton, Kalgoorlie terrane.||Kambalda Sequence||Overlies the Kapai Slate, underlies the Oroya Shale.||
26833|Paringa Basalt|73391|5|Briefly described|p19-20, 38, 109, 111, 114, 194, 230|||See also p244, 278-279, 303-304, 308, 347, Appendices. Woodall (1965). Kambalda Domain, Kalgoorlie Terrane, Eastern Goldfields Province. Thickness varies from <900m to 1500m.||Upper Basalt.||Overlies Kapai Slate. Is overlain unconformably by Talbot formation. The Golden Mile Dolerite intrudes along the contact of this unit and overlying Spargoville Formation.|Tholeiitic basalt and intercalated komatiitic basalt with interflow sedimentary rocks; local upper plagioclase-phyric flows.|
26833|Paringa Basalt|73596|6|Mentioned|p1160, 1162|||Appears as Victorious/Paringa Basalt.||Hannans Subgroup.||Overlies Kapai Slate. Is overlain by Talbot Formation (Black Flag Group).||
74599|Parker Hills Supersuite|60555|6|Mentioned|p9|||Cassidy and Champion (2002). Leucogranites to biotite-bearing monzonites, high-Ca.||||||
40793|Parker Range Member|50319|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Glenayle Dolerite. Fine- to medium-grained dolerite, commonly with pink granophyre zones.||||||
40793|Parker Range Member|64655|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Glenayle Dolerite. Fine- to medium-grained dolerite, commonly with pink granophyre zones; local superposition of sills indicated by l (lower) and u (upper).||||||17-NOV-08
40793|Parker Range Member|64772|5|Briefly described|p13|Mesoproterozoic|Mesoproterozoic|Of the Glenayle Dolerite.||||||07-FEB-11
70570|Parmelia Bank Shellsand|61521|5|Briefly described|p39 Tb.7|||Well sorted carbonate sand unit in Cockburn Sound. Geological Province: Rottnest Shelf region.||||||
40563|Parmelia Group|12758|4|Described|p18, p3 Fig. 3|Neocomian|Neocomian|Supersedes the Parmelia Formation. Geological Province: Perth basin. See also p8 Fig. 9 and p10 Fig. 10.||||||01-OCT-08
40563|Parmelia Group|14227|5|Briefly described|p8, p11|Valanginian|Berriasian|Includes Charlotte Sandstone, Carnac Formation (including Hawley, Mangles and Stragglers Members), and Otorowiri Formation. Fluvial deposits including red bed sediments. See also Enclosure 2 where age max: Tithonian, min: Berriasian.||||||07-FEB-11
40563|Parmelia Group|24443|5|Briefly described|Fig.30|Early Cretaceous|Early Cretaceous|Conformably overlies Yarragadee Formation. Overlain by Bunbury Basalt and Warnbro Group (unconformable). Geological Province: Perth Basin.||||||
40563|Parmelia Group|50107|5|Briefly described|Map legend|Cretaceous|Cretaceous|Geological Province: Perth Basin.||||||
40563|Parmelia Group|50108|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Geological Province: Perth Basin.||||||
40563|Parmelia Group|60376|5|Briefly described|p17 Fig. 4.|Early Cretaceous|Late Jurassic|Geol Prov: Perth Basin. Includes; Otorowiri Formation, Jervoise Sandstone, Carnac Formation and Charlotte Sandstone. Overlain unconformably by Gage Sandstone (Warnbro Group). Underlain uncomformably by Yarragadee Formation.||||||07-FEB-11
40563|Parmelia Group|60386|6|Mentioned|p302|Berriasian|Berriasian|Perth Basin. Non-marine.||||||
40563|Parmelia Group|61811|5|Briefly described|p3 Fig.2, p39, p65.|Berriasian|Tithonian|Northern Perth Basin. Formerly Parmelia Formation; raised to Group status by Crostella and Backhouse (2000). Type section details in p65, Appendix 1, where it is called 'Parmelia Formation'.|||Includes Otorowiri Formation.|Overlies Yarragadee Formation.||
40563|Parmelia Group|64580|4|Described|map legend|Early Cretaceous|Late Jurassic|Predominantly sandstone, most formations recognised only in subsurface.||||||15-DEC-08
40563|Parmelia Group|64635|5|Briefly described|p4 Fig.3, p23  |Berriasian|Tithonian||||Includes Otorowiri Formation.|Overlies Yarragadee Formation.||
40563|Parmelia Group|67340|5|Briefly described|p6|Early Cretaceous|Jurassic|Northern Perth Basin. Its top marks the Early Cretaceous breakup unconformity. See also references to Parmelia Formation (p7, 25, 50, 52, 60, 62).|||Otorowiri Formation.|Is overlain unconformably by South Perth Shale (Warnbro Group).||
40563|Parmelia Group|67925|5|Briefly described|Ch2 p10 fig 4, Ch4 p8 fig 2|Berriasian|Berriasian|Mistakenly referred to as the Parmelia Formation in Ch4 p8 fig 2. ||||Overlies the Yarragadee Formation. Unconformably overlain by the Warnbro Group and the Gage Sandstone.||
40563|Parmelia Group|69029|6|Mentioned|p332|Cretaceous|Tithonian|Of Perth Basin.||||Underlain by Yarragaddee Formation.||
40563|Parmelia Group|69081|5|Briefly described|p737 Fig.1|Early Cretaceous|Early Cretaceous|Geol. Prov: Perth Basin.||||Is overlain by South Perth Shale and Gage Sandstone (Warnbro Group).||23-JUL-15
40563|Parmelia Group|69182|5|Briefly described|Ch2 p3, Ch2 p9, Ch2 p15|Lower Cretaceous|Lower Cretaceous|Perth Basin. Maximum thickness of 829m. See also Ch2 p45, Ch2 p52-p53,Ch2 p55, Ch2 p60-p63, Ch2 p84-p86. |||Includes the Carnac Formation, Jervoise Sandstone, Otorowiri Formation and the Charlotte Sandstone.|Overlies the Yarragadee Formation and the Otorowiri Formation. Overlain by the Bunbury Basalt and unconformably overlain by the Warnbro Group.|Coarse-grained fluvial sandstones that alternate with fine-grained clastic sedimentary rocks.|
40563|Parmelia Group|69297|6|Mentioned|p175, p189, p223, p225, p236, p238|Berriasian|Tithonian|Vlaming Sub-basin, South Perth Basin. ||||Overlies the Yarragadee Formation. Overlain by the Bunbury Basalt.||
40563|Parmelia Group|70097|5|Briefly described|p3, p8, p19-21 Figs.3-5|Berriasian|Berriasian|Perth Basin. Dandaragan Trough, Beermullah Trough, Vlaming Sub-basin and Bunbury Trough.|||Otorowiri Formation, Jervoise Sandstone, Carnac Formation, Charlotte Sandstone|Overlies Yarragadee Formation. Is overlain by Bunbury Basalt, South Perth Shale or Gage Sandstone (Warnbro Group).|Red bed sedimentation.|12-SEP-17
40563|Parmelia Group|70099|5|Briefly described|Fig.4; p5|Berriasian|Berriasian|Vlaming Sub-basin. Correlated to Mentelle 3 and 4 syn-rift Supersequences.|||Jervoise and Charlotte Sandstones; Otorowiri and Carnac Formations.|Overlies Yarragadee Formation. Is overlain by Bunbury Basalt.||
40563|Parmelia Group|70128|5|Briefly described|p449, p456, p459-463|Early Cretaceous|Early Cretaceous|Perth Basin. Modelled thickness distribution histogram.|||Otorowiri, Carnac Formations; Jervoise Sandstone.|Conformably overlies Yarragadee Formation. Is overlain unconformably by Gage Sandstone (Warnbro Group).||
40563|Parmelia Group|70796|4|Described|2_5m_interpgeop15_lut.csv|Berriasian|Upper Jurassic|Of the Perth Basin. A minimum age is also provided of ca. 139.8 Ma; both the max and min age are biostratigraphic ages. Affected by the following events: MidMiocene transgression, 15 Ma (15  15 Ma); Wilson Bluff transgression, 42 Ma (42  42 Ma); Kings Park transgression, 56 Ma (56  56 Ma); Gondwana breakup  western margin (210  125 Ma); Jurassic  Early Cretaceous rifting, Perth Basin (168  133 Ma). See also 500k_interpgeop14_lut.csv.|163.5  139.8 Ma (biostrat)||||Predominantly sandstone; most formations recognized only in subsurface.|
40563|Parmelia Group|70826|6|Mentioned|p7 tbl 4|Early Cretaceous|Jurassic|Perth Basin.||||||
40563|Parmelia Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone, shale|
40563|Parmelia Group|71269|5|Briefly described|GEOL_LUT_CSV files|Berriasian|Late Jurassic|Of Perth Basin. Events: Mid-Miocene transgression, 15 Ma (15-15 Ma); Wilson Bluff transgression, 42 Ma (42-42 Ma); Kings Park transgression, 56 Ma (56-56 Ma); Gondwana breakup-western margin (210-125 Ma); Jurassic-Early Cretaceous rifting, Perth Basin (168-133 Ma);??. See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv. |163.5-139.8 Ma (biostrat)||||Predominantly sandstone; most formations recognized only in subsurface|
40563|Parmelia Group|71377|5|Briefly described|p7|Early Cretaceous|Late Jurassic|Perth Basin.|||Includes the Charlotte Sandstone, Carnac Formation, Jervoise Sandstone and Otorowiri Formation.|||
40563|Parmelia Group|71958|5|Briefly described|p6, p14, p20, p34-p35, p41, p51, p80|Valanginian|Berriasian|Vlaming Sub-basin, Perth Basin. Primarily composed of fluvio-lacustrine and deltaic successions. Several potential plays are described in Miyazaki et al (1996).|||Includes the Charlotte Sandstone, Carnac Formation, Jervoise Sandstone and the Otorowiri Formation.|Overlies the Yarragadee Formation. Overlain by the Warnbro Group.||
40563|Parmelia Group|72034|5|Briefly described|500k_interpgeop16_lut|Berriasian|Late Jurassic|Perth Basin.  Age from biostratigraphy.|||Includes Otorowiri Formation.||Predominantly sandstone; most formations recognized only in subsurface.|
40563|Parmelia Group|72258|5|Briefly described|p129-130,133|Early Cretaceous|Early Cretaceous|Of Perth Basin. Neoarchean (2800-2600 Ma) detrital zircons attributed to Yilgarn Craton, along eastern boundary of Perth Basin (Kositcin et al., 2008; Mole et al., 2013; Nemchin and Pidgeon, 1997). Minor distribution of Late Paleoproterozoic (1800-1600 Ma) detrital zircons correlate with characteristic ages and Hf isotopic signatures of magmatism in the Albany-Fraser-Wilkes Orogen (Clark et al., 2000; Fitzsimons, 2000, 2003; Kirkland et al., 2011; Spaggiari et al., 2015). Major peak in Mesoproterozoic (1300-1100 Ma) and minor Late Paleoproterozoic (1800-1600 Ma) detrital zircons correlate with characteristic ages and Hf isotopic signatures of magmatism in the Albany-Fraser-Wilkes Orogen (Clark et al., 2000; Fitzsimons, 2000, 2003; Kirkland et al., 2011; Spaggiari et al., 2015). Late Meso- to Early Neoproterozoic (1100-900 Ma) detrital zircons atributed to Pinjarra Orogen. Bimodal Neoproterozoic 750 and 500 Ma peaks in detrital zircon ages also likely to be derived locally from Pinjarra Orogen (p134-135 describes potential, but unlikely Gondwanan sources).||||Overlain unconformably by Bunbury Basalt or Gage Sandstone.||
40563|Parmelia Group|73424|6|Mentioned|p5|Early Cretaceous|Early Cretaceous|Perth Basin.||||||
40563|Parmelia Group|73513|5|Briefly described|p30 Fig.2|Valanginian|Berriasian|Perth Basin.||||Overlies Yarragadee Formation|Fluvial unit.|
83645|Parry Beach basaltic dyke|73480|5|Briefly described|p212-213||Stenian|Vertical and  NW striking dyke at Parry Beach/Hillier Bay. Plagioclase 40Ar/39Ar analyses from PB1 yielded a disturbed spectrum with individual steps between 1700 and 1200 Ma. See also Parry Beach dyke. Hosted in ortho- and paragneiss.|1183+/-10 Ma U-Pb zircon max. crystallisation age||||Porphyritic basalt dyke.|
27874|Paterson Formation|7433|5|Briefly described|p25 Fig.2, p33.|Permian|Permian|Canning Basin. Preserved within Permian valleys incised into Precambrian basement along the Basin's southwest margin.||||Continental lateral equivalent to the Grant Group.|Tillite.|
27874|Paterson Formation|22707|5|Briefly described|P15, Table1 P8||Sakmarian|||||||
27874|Paterson Formation|22801|6|Mentioned|P11||Permian|||||||
27874|Paterson Formation|22814|5|Briefly described|fig2|Early Permian|Early Permian|||||||
27874|Paterson Formation|22816|6|Mentioned|p43 Fig4.2|||||||||
27874|Paterson Formation|23128|5|Briefly described|p372||Permian|||||||
27874|Paterson Formation|23253|5|Briefly described|p2||Permian|See unnumbered figure.||||||
27874|Paterson Formation|23281|5|Briefly described|p7||Permian|||||||
27874|Paterson Formation|23364|5|Briefly described|map legend|Permian|Permian|Canning Basin.||||||
27874|Paterson Formation|23414|5|Briefly described|Map Legend|Permian|Permian|Canning Basin||||||
27874|Paterson Formation|23415|5|Briefly described|Map Legend|Permian|Permian|Geological province: Canning Basin. Diamictite. mudstone, siltstone, sandstone, and minor conglomerate. Fluvioglacial deposits.||||||07-JAN-08
27874|Paterson Formation|23529|4|Described|p25|Permian|Permian|Max. thickness: 100m. Geological Province: Canning Basin.||||||17-NOV-08
27874|Paterson Formation|23530|5|Briefly described|Map Legend|Permian|Permian|||||||
27874|Paterson Formation|23558|6|Mentioned|p36|||Geological Province: Officer Basin.||||||
27874|Paterson Formation|23571|5|Briefly described|p23|Carboniferous|Carboniferous|Geological Province: Officer Basin||||||
27874|Paterson Formation|23575|5|Briefly described|Map Legend|Permian|Permian|||||||
27874|Paterson Formation|23580|5|Briefly described|Map legend||Permian|||||||
27874|Paterson Formation|23581|5|Briefly described|Map legend||Permian|||||||
27874|Paterson Formation|23583|5|Briefly described|Map Legend|Permian|Permian|Overlain by Callawa Formation. Geological Province Canning Basin.||||||24-JUL-07
27874|Paterson Formation|23585|4|Described|p24|Permian|Permian|Geological Province: Canning Basin.||||||
27874|Paterson Formation|23587|4|Described|p17|Early Permian|Early Permian|Age: c. 290Ma||||||
27874|Paterson Formation|23588|4|Described|p8|Permian|Permian|||||||
27874|Paterson Formation|23590|4|Described|p17|Sakmarian|Asselian|||||||
27874|Paterson Formation|23591|6|Mentioned|p20|||Geological Province: Officer Basin.||||||
27874|Paterson Formation|23594|4|Described|p23|Permian|Permian|Underlain by Pinjian Chert Breccia. Geological Province: Canning Basin. Max. thickness: >140 m.||||||24-JUL-07
27874|Paterson Formation|23596|5|Briefly described|p20|||Geological Province: Officer Basin.||||||
27874|Paterson Formation|23602|4|Described|p18|Permian|Permian|||||||
27874|Paterson Formation|23611|5|Briefly described|p21|Permian|Permian|See also page 33 Appendix 1. Geological Province: Gunbarrel Basin.||||||
27874|Paterson Formation|23742|6|Mentioned|p1|||||||||
27874|Paterson Formation|23745|4|Described|p19|Early Permian|Early Permian|Geological Province: Canning Basin.||||||
27874|Paterson Formation|23746|4|Described|p28|Permian|Permian|Geological Province: Canning Basin||||||
27874|Paterson Formation|23757|4|Described|p15-16|Early Permian|Early Permian|Overlies Cooieena Basalt and underlies, unconformably, the Callawa Formation. Fluvioglacial rocks - consist of sandstone, pebble conglomerate and diamictite carrying occasional striated and faceted cobbles and small boulders.|||||Fluvioglacial rocks - consist of sandstone, pebble conglomerate and diamictite carrying occasional striated and faceted cobbles and small boulders.|02-OCT-09
27874|Paterson Formation|23758|4|Described|p11|Permian|Permian|||||||
27874|Paterson Formation|23760|4|Described|p33|Permian|Permian|Geological Province: Canning Basin.||||||
27874|Paterson Formation|23796|5|Briefly described|p87|Early Permian|Early Permian|Max Thickness: >80m||||||
27874|Paterson Formation|23989|6|Mentioned|p51|Permian|Permian|Geological Province: Yilgarn Craton||||||
27874|Paterson Formation|24025|5|Briefly described|p16|Permian|Permian|Geological Province: Canning Basin.||||||
27874|Paterson Formation|24067|5|Briefly described|p252|Permian|Permian|Geological Province: Officer Basin.||||||
27874|Paterson Formation|24110|5|Briefly described|Plate 1|Permian|Permian|Geological Province: Canning Basin||||||
27874|Paterson Formation|24135|5|Briefly described|p44|Permian|Permian|Geological Province: Officer Basin.||||||
27874|Paterson Formation|24161|4|Described|p9 Fig. 6, p26, p28|Early Permian|Late Carboniferous|Unconformably overlain by the Samuel Formation. Geological Province: Gunbarrel Basin.||||||
27874|Paterson Formation|24183|5|Briefly described|p6|Permian|Permian|||||||
27874|Paterson Formation|24244|5|Briefly described|p2 fig 1, p3|Early Permian|Early Permian|Gunbarrel Basin. Flat-lying, glacially influenced deposit.|||||Claystone, sandstone, poorly sorted conglomerate.|
27874|Paterson Formation|24390|5|Briefly described|p11 Fig. 6|Permian|Permian|Geological Province: Gunbarrel Basin.||||||
27874|Paterson Formation|24494|5|Briefly described|p24, p37 App.1|Permian|Permian|Geological Province: Gunbarrel Basin.||||||
27874|Paterson Formation|30008|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|30009|4|Described|p13|||||||||
27874|Paterson Formation|30012|6|Mentioned|Table 1|||||||||
27874|Paterson Formation|30340|6|Mentioned|p2533|||||||||
27874|Paterson Formation|30341|4|Described|p145|||||||||
27874|Paterson Formation|30971|6|Mentioned|Map legend|Early Permian|Early Permian|Prob.Lower Permian||||||
27874|Paterson Formation|30974|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|30975|6|Mentioned|Map legend|Permian|Permian|||||||
27874|Paterson Formation|30977|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|31091|6|Mentioned|p20|||||||||
27874|Paterson Formation|31092|6|Mentioned|p4|||||||||
27874|Paterson Formation|31455|6|Mentioned|Table 2|||||||||
27874|Paterson Formation|31456|4|Described|Table 1|||||||||
27874|Paterson Formation|31457|4|Described|Table 2|||||||||
27874|Paterson Formation|31458|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|31459|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|31460|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|31562|4|Described|p9|||Stratigraphic table p10.||||||24-JUL-07
27874|Paterson Formation|31632|4|Described|Table 2|||See also p11.||||||24-JUL-07
27874|Paterson Formation|31633|4|Described|Table 2|||Mention p6.||||||24-JUL-07
27874|Paterson Formation|31634|4|Described|Table 1|||See also pp5,6.||||||
27874|Paterson Formation|31635|4|Described|Table 2|||||||||
27874|Paterson Formation|31636|5|Briefly described|p7|||See also Table 2||||||
27874|Paterson Formation|31638|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|31639|6|Mentioned|Map legend|Permian|Permian|||||||
27874|Paterson Formation|31640|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|31641|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|31642|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
27874|Paterson Formation|31914|2|Defined|p98|Permian|Permian|Replaces Wilkinson Range Beds and Yowalga Sandstone in Officer Basin.||||||24-JUL-07
27874|Paterson Formation|32648|6|Mentioned|p32|||L.Permian||||||
27874|Paterson Formation|33586|4|Described|Table 1|||See also p13.||||||24-JUL-07
27874|Paterson Formation|33587|3|Fully described|p7|||See also Table 2.||||||
27874|Paterson Formation|33588|4|Described|Table 2|||See also p8.||||||24-JUL-07
27874|Paterson Formation|33589|6|Mentioned|p7|||Permian||||||
27874|Paterson Formation|33590|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|33591|5|Briefly described|p9|||||||||
27874|Paterson Formation|33592|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|33595|4|Described|Table 1|||||||||
27874|Paterson Formation|33596|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|33597|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
27874|Paterson Formation|34742|6|Mentioned|Map legend|Permian|Permian|||||||
27874|Paterson Formation|34917|6|Mentioned|Fig. 2|||||||||
27874|Paterson Formation|35123|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|35127|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|35201|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|35207|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|35222|4|Described|Table.2|||||||||
27874|Paterson Formation|35223|4|Described|Table.2|||||||||
27874|Paterson Formation|35226|4|Described|Table 1|||||||||
27874|Paterson Formation|35250|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|35251|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|35252|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|35387|6|Mentioned|Map legend|Permian|Permian|||||||
27874|Paterson Formation|35496|4|Described|Table 1|||Also p19.||||||24-JUL-07
27874|Paterson Formation|35497|4|Described|Table 1|||Also on p10.||||||24-JUL-07
27874|Paterson Formation|35596|4|Described|p13|||||||||
27874|Paterson Formation|35642|6|Mentioned|Map legend|Early Permian|Early Permian|Prob.Lower Permian||||||
27874|Paterson Formation|35902|4|Described|Table 1|||||||||
27874|Paterson Formation|35903|4|Described|Table 1|||||||||
27874|Paterson Formation|36257|6|Mentioned|Table 2.1|||||||||
27874|Paterson Formation|36632|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|36701|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|36890|3|Fully described|p405|||Formerly Paterson Range Series. See also p342.||||||24-JUL-07
27874|Paterson Formation|36899|6|Mentioned|p1089|||||||||
27874|Paterson Formation|37019|6|Mentioned|Map legend|Early Permian|Early Permian|Prob.Lower Permian||||||
27874|Paterson Formation|37021|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|37022|6|Mentioned|Map legend|Permian|Permian|||||||
27874|Paterson Formation|37023|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|37106|6|Mentioned|Fig.2|||||||||
27874|Paterson Formation|37212|3|Fully described|p16|||||||||
27874|Paterson Formation|37484|6|Mentioned|p411|||||||||
27874|Paterson Formation|37914|5|Briefly described|p450|||See also p449.||||||08-FEB-10
27874|Paterson Formation|37916|3|Fully described|p464|||Formerly Wilkinson Range Beds.||||||
27874|Paterson Formation|37926|6|Mentioned|p500|||||||||
27874|Paterson Formation|38516|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|38768|6|Mentioned|p83|||||||||
27874|Paterson Formation|38878|6|Mentioned|Map legend|Sakmarian|Sakmarian|||||||
27874|Paterson Formation|38898|6|Mentioned|p84|||||||||
27874|Paterson Formation|39424|6|Mentioned|Map legend|Permian|Permian|||||||
27874|Paterson Formation|39426|4|Described|p14|||||||||
27874|Paterson Formation|39697|4|Described|p137|||||||||
27874|Paterson Formation|39854|6|Mentioned|p18|||||||||
27874|Paterson Formation|39857|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|40089|6|Mentioned|p17|||||||||
27874|Paterson Formation|40170|6|Mentioned|p150|||||||||
27874|Paterson Formation|40354|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|40355|6|Mentioned|p11|||||||||
27874|Paterson Formation|40934|6|Mentioned|Map legend|Permian|Permian|||||||
27874|Paterson Formation|40938|6|Mentioned|p5|||||||||
27874|Paterson Formation|41125|6|Mentioned|p40|||||||||
27874|Paterson Formation|41669|3|Fully described|p51|||||||||
27874|Paterson Formation|41839|6|Mentioned|p26|||||||||
27874|Paterson Formation|42278|6|Mentioned|p33|||||||||
27874|Paterson Formation|42431|5|Briefly described|p235|||Officer Basin||||||
27874|Paterson Formation|42547|4|Described|p97|||||||||
27874|Paterson Formation|42548|5|Briefly described|p52|||||||||
27874|Paterson Formation|42613|5|Briefly described|P 2, P 13|||Part equivalent of Grant Group||||||
27874|Paterson Formation|42702|5|Briefly described|map legend|Permian||||||||
27874|Paterson Formation|42708|5|Briefly described|Plate 1|Early Permian||||||||
27874|Paterson Formation|42711|6|Mentioned|p19|||Geological province: Officer Basin. Equivalent to Shotts Formation in the Collie Basin.||||||11-AUG-08
27874|Paterson Formation|42724|5|Briefly described|map legend|Permian||||||||
27874|Paterson Formation|42734|5|Briefly described|map legend|Permian||||||||
27874|Paterson Formation|42816|6|Mentioned|p17|||||||||
27874|Paterson Formation|42817|5|Briefly described|p27|||||||||
27874|Paterson Formation|43055|5|Briefly described|p30|||||||||
27874|Paterson Formation|43056|5|Briefly described|Map Legend|||||||||
27874|Paterson Formation|43067|5|Briefly described|Fig.12,p124,p120|||||||||
27874|Paterson Formation|43118|5|Briefly described|Table 1|||||||||
27874|Paterson Formation|43348|5|Briefly described|P10, p12, p13||Phanerozoic|||||||
27874|Paterson Formation|43442|6|Mentioned|p32|Permian|Carboniferous|||||||
27874|Paterson Formation|43595|6|Mentioned|Fig 3-43,p348||Permian|||||||
27874|Paterson Formation|43605|6|Mentioned|p2||Permian|||||||
27874|Paterson Formation|43756|6|Mentioned|Fig.1,p534,541|Permian|Carboniferous|||||||
27874|Paterson Formation|43816|6|Mentioned|p87|||||||||
27874|Paterson Formation|43818|6|Mentioned|Fig.2.p39|Early Permian|Late Carboniferous|Grant Group possible parent?||||||
27874|Paterson Formation|43847|5|Briefly described|Map Legend||Permian|||||||
27874|Paterson Formation|43848|5|Briefly described|Map Legend||Permian|||||||
27874|Paterson Formation|43849|5|Briefly described|Map Legend||Permian|||||||
27874|Paterson Formation|44133|6|Mentioned|p77|||||||||
27874|Paterson Formation|44143|4|Described|p.436 Table 4-19, p445|Permian|Permian|Up to 150m thick; claystone and siltstone; initially lacustrine and then fluvial under the influence of a glacial climate. Type section in the Paterson Range (PATERSON RANGE: 21deg 45' 00" S, 122deg 10' 00" E). Forms local glacial pavements.||||||24-NOV-17
27874|Paterson Formation|44145|6|Mentioned|p548|Early Permian|Early Permian|Regarded as Officer Basin.||||||
27874|Paterson Formation|44149|6|Mentioned|p83-84 Tb.2-8|||||||||
27874|Paterson Formation|44189|5|Briefly described|Map legend||Permian|||||||
27874|Paterson Formation|44190|5|Briefly described|Map Legend||Permian|||||||
27874|Paterson Formation|44229|5|Briefly described|Map Legend|Permian|Permian|Diamictite, mudstone, siltstone, sandstone and minor conglomerate.||||||10-NOV-04
27874|Paterson Formation|44354|5|Briefly described|Map Legend||Early Permian|||||||
27874|Paterson Formation|44357|4|Described|p12,Tb.1 p9||Permian|Subsurface only. Crops out on Paterson sheet area, to the south.||||||
27874|Paterson Formation|44443|5|Briefly described|map legend|Early Permian|Early Permian|||||||
27874|Paterson Formation|44479|2|Defined|p.8|||E/51-1.||||||
27874|Paterson Formation|44499|14|Not recorded|opp.p.6, Tb.1||Permian|||||||
27874|Paterson Formation|44831|5|Briefly described|Map Legend||Permian|||||||
27874|Paterson Formation|44865|5|Briefly described|Map Legend||Permian|||||||
27874|Paterson Formation|44866|5|Briefly described|Map Legend||Permian|||||||
27874|Paterson Formation|44994|6|Mentioned|Fig.1|||Permian. Correlation||||||
27874|Paterson Formation|44998|2|Defined|p.74-8|Sakmarian|Stephanian|Underlies Cronin Sandstone, Cuncudgerie Sandstone. Sakmarian-U.Stephanian. See also p80-2,102-4, map, App.1 p257,261.||||||
27874|Paterson Formation|45016|14|Not recorded|p.18|||Glaciation.||||||
27874|Paterson Formation|45104|5|Briefly described|p27|||||||||
27874|Paterson Formation|45149|2|Defined|p44|Early Permian|Early Permian|See also p3 and Table 1.||||||24-JUL-07
27874|Paterson Formation|45153|2|Defined|App.4-63|early Sakmarian|early Sakmarian|Formerly called "Paterson Range Series".||||||
27874|Paterson Formation|45158|3|Fully described|p22|||See also p13. Sakmarian microfossils.||||||14-OCT-08
27874|Paterson Formation|45168|6|Mentioned|p6|||||||||
27874|Paterson Formation|46319|4|Described|p16|Early Permian|Early Permian|Maximum thickness: 250m.  Geological Province: Canning Basin.||||||
27874|Paterson Formation|46849|6|Mentioned|p189|||||||||
27874|Paterson Formation|46975|6|Mentioned|Fig.2|||||||||
27874|Paterson Formation|48826|14|Not recorded|Tb.III|||Correlates with Grant Formation.||||||
27874|Paterson Formation|48842|14|Not recorded|Tb.I.|||||||||
27874|Paterson Formation|49644|5|Briefly described|Table|||||||||
27874|Paterson Formation|49895|4|Described|p10|Permian|Permian|Geological Province: Canning and Gunbarrel Basins. Overlain disconformably by Cronin Sandstone. See also p6 Fig.3.||||||02-OCT-09
27874|Paterson Formation|49911|5|Briefly described|Map legend|Permian|Permian|Sandstone, claystone, conglomerate and boulder beds; tillite and other fluvioglacial deposits.  Geological Province: Canning Basin||||||
27874|Paterson Formation|50085|5|Briefly described|p11 Fig. 6|Permian|Carboniferous|Age: ~300Ma.  Geological Province: Officer Basin.||||||
27874|Paterson Formation|50189|4|Described|p27|Sakmarian|Asselian|Basal unit of pebble to boulder-bearing diamictite (possibly tillite), overlain by interbedded sandstone, siltstone, shale, and conglomerate. Unconformably overlain by Callawa Formation. Geological Province: Lambert Shelf.||||Unconformably overlain by Callawa Formation|Basal unit of pebble to boulder-bearing diamictite (possibly tillite), overlain by interbedded sandstone, siltstone, shale, and conglomerate|24-NOV-09
27874|Paterson Formation|50195|5|Briefly described|Map Legend|Permian|Permian|Poorly sorted sandstone, siltstone and polymitic conglomerate; glacigene.||||||23-JUN-04
27874|Paterson Formation|50204|5|Briefly described|p49 Fig.1, p51, p56|Early Permian|Early Permian|Of the Gunbarrel Basin. Flat-lying; glacially influenced. Unconformably overlies Neoproterozoic to ?Cambrian siliciclastic and calcareous sedimentary rocks, which are probably equivalent to the Kanpa Formation.|||||Mainly claystone, sandstone and poorly sorted conglomerate. Includes large granitic boulders.|06-FEB-18
27874|Paterson Formation|50205|5|Briefly described|p59 Fig.1,|Permian|Permian|Of Gunbarrel Basin. ?300 Ma.||||||
27874|Paterson Formation|50287|5|Briefly described|Map Legend|Permian|Permian|Geological Province: Canning Basin. Sandstone, siltstone, and mudstone; diamictite; fluvioglacial deposits.||||||31-MAY-04
27874|Paterson Formation|50378|5|Briefly described|Map Legend|Permian|Permian|Geological Province: Gunbarrel Basin. Poorly sorted sandstone, claystone, and conglomerate; glacigene to fluvioglacial.||||||22-JUN-04
27874|Paterson Formation|50544|3|Fully described|p63|Early Permian|Early Permian|Fluvioglacial deposits. Mesas unconformably overlie Pinjian Chert Breccia; patches of this formation unconformably underlie the Callawa Formation. Geological Province: Canning Basin. See also p14.||||||26-MAY-09
27874|Paterson Formation|50555|5|Briefly described|Map legend|Permian|Permian|Diamictite, mudstone, siltstone, sandstone, and minor conglomerate.  Overlies Pinjian Chert Breccia and Carawine Dolomite.  Geological Province: Canning Basin.||||||22-JUL-04
27874|Paterson Formation|60429|4|Described|p7, p27|Permian|Permian|Unconformably overlain by Callawa Formation. Geological Province: Canning Basin. Basal unit is pebble- to cobble-bearing diamictite. Further lithology is included. See also p8 Fig. 4.||||||07-FEB-11
27874|Paterson Formation|60470|5|Briefly described|p9, 10-11|Permian|Permian|Overlies Lamil Formation||||||
27874|Paterson Formation|61023|5|Briefly described|p15 Fig. 8|Permian|Carboniferous|Geological Province: Gunbarrel Basin. See also p16 Tb. 3.||||||11-APR-08
27874|Paterson Formation|61197|5|Briefly described|p474 Fig.2|Permian|Permian|Glacial sediments filling tunnel valleys set into Precambrian basement.|||||Bouldery diamictite.|
27874|Paterson Formation|61732|5|Briefly described|p86|Permain|Permian|Overlies Turkey Hill Formation.||||||07-FEB-11
27874|Paterson Formation|62453|5|Briefly described|p6 Fig. 4, 21, 22|||Overlies Durba Sandstone. Unconformably overlies: Turkey Hill Formation.||||||24-JUL-07
27874|Paterson Formation|63022|5|Briefly described|p1016 Fig. 2|?Permian|Late Carboniferous|Clay, grey mudstone, grey to brown sandstone, minor conglomerate. ||||||
27874|Paterson Formation|63139|5|Briefly described|p50|Permian|Permian|Fluvio-glacial deposits.||||||
27874|Paterson Formation|63417|5|Briefly described|Map legend|Permian|Carboniferous|Geological Province: Canning Basin. Conglomerate (including diamictite), sandstone and siltstone; largely glacigene.||||||
27874|Paterson Formation|64103|6|Mentioned|p401|Permian|Carboniferous|Glacigene.||||||07-FEB-11
27874|Paterson Formation|64325|5|Briefly described|p82 Fig. 2, p86|Permian|Permian|Geological Province:Gunbarrel  Basin.||||||26-AUG-08
27874|Paterson Formation|64580|4|Described|map legend|Early Permian|Pennsylvanian|Conglomerate (including diamictite), sandstone and siltstone; largely glacigene.||||||15-DEC-08
27874|Paterson Formation|64586|5|Briefly described|Map legend|Permian|Permian|Fluvial sandstone, siltstone, conglomerate; lacustrine claystone and siltstone; glacigene conglomerate, sandstone and siltstone.|||||Fluvial sandstone, siltstone, conglomerate; lacustrine claystone and siltstone; glacigene conglomerate, sandstone and siltstone.|23-DEC-09
27874|Paterson Formation|64630|5|Briefly described|p31 Fig.2|Sakmarian|Gzhelian|Province: Gunbarrel and Canning Basins. Palynology age: D. tenuistriatus to P. confluens. Lithology: mixed succession of diamictite, sandstone and siltstone. Inferred glacial influence.||||||
27874|Paterson Formation|64655|5|Briefly described|Map Legend|Permian|Permian|Geological Province: Gunbarrel Basin.|||||Poorly sorted sandstone; minor conglomerate and siltstone; glacigene|02-OCT-09
27874|Paterson Formation|64772|4|Described|p16, Plate 1, p35 Fig. 23|Permian|Carboniferous|Geological province: Gunbarrel Basin (Officer Basin) and Canning Basin. Unit originally defined for Permian sedimentary rocks of the southern Canning Basin (Talbot, 1920; Traves et al., 1956) and later extended by Lowry et al. (1972) to the Officer Basin. Unconformable relationship with older rocks regionally, but local relationships are sometimes complicated by the similarity in lithology and orientation of underlying units (Hocking et al., 2001a).  See also p20-21 Fig.10, p26 Fig.13, p26 Fig.14, p27 Fig.15, p29 Fig.17, p32 Fig.19, p46 Fig.34, p75 App.4 Tb.4.3, p76-77 Fig.4.2, p78 App.4 Tb.4.4, p79-81 App.4 Fig.4.3,||||Overlies, and contains clasts of, Frere Formation; overlies Chiall Formation; see Comments.|Conglomerate (diamictite), sandstone, and claystone, representing glacial, fluviatile, and glaciolacustrine environments. Detailed variable lithology descriptions provided.|25-NOV-13
27874|Paterson Formation|64793|6|Mentioned|p286 Fig.5|Paleozoic|Paleozoic|||||||
27874|Paterson Formation|64970|5|Briefly described|p719, p719 Fig. 2, p720, p721 Fig. 7|Early Permian|Carboniferous|Equated to the Grant Group of the Canning Basin. Geological Province: Officer Basin. Tillites, fluvioglacial to lacustrine sandstone and claystone. ||||||
27874|Paterson Formation|65102|4|Described|p.366,369,374,378, Figs4-41,4-49|Early Permian|Early Permian|Officer Basin. 100-450m; fine-grained sandstone to claystone, siltstone, coarse pebbly sandstone & diamictite; glacial, fluvial & lacustrine; disconformable on all older rocks; type section in Paterson Range, 21deg 45min S, 122deg 10min E, contains Asselian palynomorphs.||||||
27874|Paterson Formation|65180|5|Briefly described|map legend|Permian|Carboniferous|Conglomerate (including diamictite), sandstone, siltstone. Of the Gunbarrel Basin.||||||
27874|Paterson Formation|65194|5|Briefly described|p5 Fig.1.3|Permian|Permian|Bouldery diamictite; glacial basin bedrock surface in Roe drainage basin.||||||
27874|Paterson Formation|65259|5|Briefly described|Map legend|Permian|Permian|Interbedded Coarse-grained sandstone and mudstone.||||||
27874|Paterson Formation|65263|6|Mentioned|p20|Permian||Sandstone facies; in the Officer Basin. Arkosic sandstone and conglomerate in the Duketon 1:100k area is considered to be equivalent to this unit.||||||
27874|Paterson Formation|65264|5|Briefly described|p27, p43 Appdx. 1|Permian|Permian|Geological province: Gunbarrel Basin. Comprises conglomerate with greenstone clasts in a clay- and silt-rich matrix; shale and sandstone units, locally with dropstones; pebbly sandstone, etc.  Detailed lithology discussed.||||||07-FEB-11
27874|Paterson Formation|65363|5|Briefly described|p1, pp5-6. |Permian|Late Carboniferous|Gunbarrel Basin. Mainly fluvial; glacial diamictites are absent. Porosity and permeability are briefly discussed.||||Unconformably overlies Lungkarta Formation.|Grey claystone weathering to yellow, pale-green and pink; grey mudstone with local minor carbonaceous material; grey to brown, medium- to coarse-grained, cross-bedded sandstone; minor basal conglomerate.|
27874|Paterson Formation|65364|5|Briefly described|p81|||Gunbarrel Basin.||||Underlain by Durba Sandstone.|Clay, grey mudstone, grey to brown sandstone, minor conglomerate.|16-MAR-12
27874|Paterson Formation|65371|5|Briefly described|p53, 54 Fig. 1, p55-57, p58|||Gunbarrel Basin. Unconformably overlies ?Durba Sandstone. Clay, mudstone sandstone and minor conglomerate. Interpreted glacio-fluvial depositional environment. From the Gunbarrel Basin. Mineralogy discussed.||||||
27874|Paterson Formation|65403|5|Briefly described|p15.|Permian|Permian|Outcrops as isolated mesas or partially dissected benches flanking larger hills. Glacial striae on underlying rocks indicate ice movement was northerly.|||||Tillite, with well-rounded boulders locally >5 m diameter; passing upward into cross-bedded, medium- to coarse-grained sandstone, siltstone and mudstone, with ripple marks and graded laminae.|
27874|Paterson Formation|65416|5|Briefly described|p137, p138 Fig.3, p139 Fig.4, p145, p146|Early Permian|Late Carboniferous|Officer Basin. Part of Sequence Pz5. Widespread glacial sediments. At least 1200 m thick in Yowalga Sub-basin. Fluvioglacial to lacustrine environment in WA; marine in SA.||||Unconformably overlies Lennis and Durba Sandstones, Browne and McFadden Formations and Table Hill Volcanics.|Interbedded grey to red sandstones, claystone and minor tillite.|
27874|Paterson Formation|65724|5|Briefly described|map legend|Permian|Carboniferous|Unconformable over Pinjian Chert Breccia, Carawine Dolomite and Jeerinah Formation. Diamictite, mudstone, siltstone, sandstone and conglomerate; fluvioglacial deposit. Geol. Prov: Canning Basin.||||||
27874|Paterson Formation|65725|5|Briefly described|Map legend|Permian|Carboniferous|In diagrammatic section, overlies units of Throssell Range and Lamil Groups. Sandstone, mudstone, conglomerate and boulder conglomerate, tillite and other fluvioglacial deposits. Province: Canning Basin||||||26-FEB-13
27874|Paterson Formation|65825|5|Briefly described|p24.|||Permian-Carbonifereous. Fluvioglacial deposits.||||Overlies Pinjian Chert Breccia.|Basal diamictite with scattered boulders, and polished grooved pavements on underlying rocks.|
27874|Paterson Formation|65826|5|Briefly described|pp1-2, p16.|Permian|Carboniferous|Canning Basin. Fluvio-glacial sediments in palaeovalleys. Covers the poorly exposed Waukarlycarly Embayment, a graben-like structure containing at least 3 km of Phanerozoic sedimentary rocks.|||||Fluvioglacial and diamictite deposits comprising boulder to pebble conglomerate, cross-bedded and coarse-grained sandstone, and mudstone.|
27874|Paterson Formation|65828|5|Briefly described|Map legend|Permian|Permian|Canning Basin.|||||Sandstone, siltstone and mudstone; diamictite; fluvioglacial deposits.|
27874|Paterson Formation|65829|4|Described|p1, p7 Fig.3, p10, p23, pp29-30. |Permian|Carboniferous|Fluvioglacial deposits. Palynology samples suggest a Late Sakmarian age. Invariably overlain by eluvial deposit of residual boulders, cobbles and pebbles in clay, silt and sand.||||Is overlain disconformably by Oakover Formation.|Basal diamictite or polymictic conglomerate, pebbly sandstone; interbedded sandstone, siltstone and white claystone; cross-bedding common in sandstone, polished and faceted boulders in diamictite; locally forms a ferruginous duricrust surface.|
27874|Paterson Formation|65899|5|Briefly described|Map legend|Permian|Carboniferous|Gunbarrel Basin. Conglomerate (including diamictite), sandstone, siltstone; largely glacigene.||||||
27874|Paterson Formation|66113|5|Briefly described|Map legend|Permian|Carboniferous|Gunbarrel Basin. Conglomerate (including diamictite), sandstone, and siltstone; largely glacigene.||||||
27874|Paterson Formation|66117|5|Briefly described|Map legend|Permian|Carboniferous|Gunbarrel Basin. Conglomerate (including diamictite), sandstone and siltstone; largely glacigene.||||||
27874|Paterson Formation|66119|5|Briefly described|Map legend|Permian|Carboniferous|Gunbarrel Basin. Conglomerate (including diamictite), sandstone, siltstone; largely glacigene.||||||
27874|Paterson Formation|66120|5|Briefly described|Map legend|Permian|Carboniferous|Conglomerate (including diamictite), sandstone and siltstone; largely glacigene.||||||
27874|Paterson Formation|66121|5|Briefly described|Map legend|Permian|Carboniferous|Conglomerate (including diamictite), sandstone and siltstone; largely glacigene.||||||
27874|Paterson Formation|66427|6|Mentioned|p71, |||||||||
27874|Paterson Formation|66949|4|Described|p8-9, p11, p57 Appx.3|Sakmarian|Gzhelian|Type section detailed. Up to 150m thick; initially lacustrine then fluvial deposits under glacial influence: local striated pavements. Suggested equivalence with Grant Group and possible inclusion within that unit. Braeside Tillite (Clapp, 1925; Traves et al., 1956) is now considered part of Paterson Formation (Crowe and Turner, 1976). Hosts significant manganese deposits in tunnel valleys at Woodie Woodie.|||||Basal diamictite, immature sandstone, claystone and siltstone.|02-NOV-15
27874|Paterson Formation|67183|5|Briefly described|p643 Fig.3, p648|Permian|Carboniferous|Williams 1989||||Unconformably overlain by Oakover Formation; unconformably underlain by Tarcunyah Group.|Glacial clay, sands, diamictite.|
27874|Paterson Formation|67195|4|Described|p10 fig 6, p19 table 1 ,p40,  p44, 47 |Permian|Permian|Gunbarrel Basin. Thermal conductivity of 2.58 W/mK.  Basal unit of 2 wells in this study. See also App 1, App 2.|||||Diamictite; medium grained sandstone. Coarse grained to granule sized, matrix supported, pebble conglomerate, coarse grained sandstone matrix. Siltstone tillite with pebble granodiorite clasts.|
27874|Paterson Formation|67200|5|Briefly described|app 2 p8, p9||||||||Medium grained sandstone, matrix supported pebble conglomerate with coarse grained sandstone matrix.|
27874|Paterson Formation|67202|3|Fully described|p43, p44 Fig.2.10, p66-69, p74, p118-119|Permian|Permian|See also p125-126, p128, p135-137, p141, p149, p161, p174, p196, p221, p248, p252-254, p256-258, p272-273, p278, p281. One of the dominant aquifers in the Canning Basin. Fluvioglacial deposits. Over 400m thick; 33m thick at the type section. Included in Grant Group by Towner et al. (1980) and Chin et al. (1982), but described as "probably a correlative of parts of the Grant Group (Towner and Gibson, 1980)". Has a well-developed siliceous duricrust. Conductivity images, discussion. Basal tillite sourced from local Rudall Complex, inter alia.||Of Grant Group?||Unconformably overlies Broadhurst, Waltha Woora Formations. Is overlain by Poole Sandstone or Oakover Formation.|Sandstone, mudstone, conglomerate, tillite; dropstones.|22-JAN-20
27874|Paterson Formation|67454|5|Briefly described|p563. |Permian|Late Carboniferous|Gunbarrel Basin.||||Overlies Durba Sandstone.||
27874|Paterson Formation|67856|6|Mentioned|p347 tab 4-9,  p348|Permian|Permian|Of Canning and Officer Basins.||||Correlated with Buck Formation and Ligertwood beds.||
27874|Paterson Formation|68186|5|Briefly described|p60, Plates 1A, 2|Permian|Carboniferous|Gunbarrel Basin. At least 300m thick.|318-270 Ma.||||Undeformed sandstones, mudstones, and conglomerates with facetted and striated clasts, no sorting or bedding (interpreted as glacigene, i.e. tillites).|
27874|Paterson Formation|68270|5|Briefly described|p684|Permian|Permian|Western Officer Basin. See reference to Patterson Formation (same unit)  p678.||||Underlain unconformably by Turkey Hill Formation.||13-JUL-21
27874|Paterson Formation|68902|4|Described|p7, p9-10, p25-26|||Traves et al. (1956). Canning Basin, as well as Gunbarrel Basin (where it is up to 450m thick) and scattered across much of the West Australian craton, particularly the Eastern Goldfields Province. Is not distinguished from the Grant Group in subsurface studies. Distinguishing it from Poole Sandstone is not straightforward. Correlative rocks in the Oakover Valley were called the Braeside Tillite (name abandoned). Up to 100m thick in glacial palaeochannels. Overlies the siilcified unconformity surface above the Yeneena Basin succession.||Grant Group||Unconformably overlies the Lamil and Throssell Range Groups. Is overlain by the Grant Group.||18-JAN-17
27874|Paterson Formation|69009|5|Briefly described|Map Legend|Permian|Carboniferous|Canning Basin.|||||Comprises conglomerate (including diamictite), sandstone, and siltstone; largely glacigene.|
27874|Paterson Formation|69029|6|Mentioned|p329|Permian|Carboniferous|Of Officer Basin.||||Underlain unconformably by Wanna Formation.||
27874|Paterson Formation|69091|5|Briefly described|p37, p44-45, see comments|Permian|Carboniferous|Officer Basin. Thinner on top of the Browne salt wall than in surrounding areas. See also p54 Fig.4.2, p106 Fig.5.7a, p107 Fig.5.8a, p109 Fig.5.10, p116.||||Overlies Lennis Sandstone and Wanna Formation.|Glacigene; sedimentary rocks.|07-OCT-14
27874|Paterson Formation|69152|4|Described|GEOL_LUT_CSV files + geochron files|Cisuralian|Pennsylvanian|Gunbarrel Basin|||||conglomerate (including diamictite), sandstone, and siltstone; largely glacigene|
27874|Paterson Formation|69153|5|Briefly described|GEOL_LUT_CSV files|Sakmarian|Pennsylvanian||||||Conglomerate (including diamictite), sandstone, and siltstone; largely glacigene|
27874|Paterson Formation|69167|4|Described|geologyp_lut.csv|Sakmarian|Pennsylvanian||||||Conglomerate (including diamictite), sandstone, and siltstone; largely glacigene.|
27874|Paterson Formation|69182|6|Mentioned|Ch4 p3|||Canning Basin. ||||||
27874|Paterson Formation|69185|4|Described|GEOL_LUT_CSV files|Early Permian|Pennsylvanian|Of Canning Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|||||Conglomerate (including diamictite), sandstone and siltstone; largely glacigene|
27874|Paterson Formation|69386|6|Mentioned|p7|||Gunbarrel Basin. Up to >700m thick.||||||
27874|Paterson Formation|69445|6|Mentioned|p30:17|||Officer Basin.||||Overlies Table Hill Volcanics.||12-JUL-16
27874|Paterson Formation|69590|4|Described|GEOL_LUT_CSV files|Sakmarian|Pennsylvanian|Of Gunbarrel Basin, Canning Basin. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|323-290 Ma (biostrat)||||Conglomerate (including diamictite), sandstone, and siltstone; largely glacigene|
27874|Paterson Formation|69606|5|Briefly described|p4 fig 2, p18|Permian|Carboniferous|Canning Basin. |||||Glacial diamictite, sandstone, siltstone and conglomerate.|
27874|Paterson Formation|69632|5|Briefly described|p12, p14, p16, p20, p21, p25|Permian|Carboniferous|Gunbarrel Basin. Crops out in the Mulga Rock area, the site for passive seismic acquisition. Mainly fluvial deposits and glacial diamictites. Up to >700m thick.|||||Diamictite, claystone, mudstone, sandstone and conglomerate.|09-OCT-18
27874|Paterson Formation|69655|6|Mentioned|p6|||||||||
27874|Paterson Formation|69729|6|Mentioned|p68|||||||||
27874|Paterson Formation|69743|6|Mentioned|p191|Permian|Carboniferous||||||Sedimentary cover sequences.|
27874|Paterson Formation|70089|6|Mentioned|p263|Permian|Permian|Gunbarrel Basin.|||||Conglomerate, sandstone and siltstone.|
27874|Paterson Formation|70137|5|Briefly described|Map legend.|Permian|Carboniferous|Canning Basin.|||||Conglomerate (including diamictite), sandstone and siltstone; largely glacigene.|
27874|Paterson Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Sakmarian|Pennsylvanian|Canning Basin. See also 100k_geologyp14_lut.csv;  500k_interpgeop14_lut.csv; and minerie_100k_geologyp_lut.csv.|323.2 - 290.1 Ma (biostratigraphy).||||Polymictic, poorly sorted, fluvioglacial conglomerate (including diamictite), sandstone, and siltstone; largely glacigene.|
27874|Paterson Formation|70256|5|Briefly described|p5-6|Permian|Permian|Gunbarrel Basin.|||||Conglomerate, sandstone and siltstone.|
27874|Paterson Formation|70619|5|Briefly described|map legend|Permian|Carboniferous|Canning Basin.|||||Conglomerate (including diamictite), sandstone, and siltstone; largely glacigene.|18-JAN-17
27874|Paterson Formation|70634|4|Described|100k_geologyp_lut,csv|Sakmarian|Pennsylvanian||323.2 Ma- 290.1 Ma (Biostratigraphy)||||Conglomerate (including diamictite), sandstone, and siltstone; largely glacigene|
27874|Paterson Formation|70762|5|Briefly described|Map legend.|Permian|Carboniferous|Canning Basin.|||||Conglomerate (including diamictite), sandstone and siltstone; largely glacigene.|
27874|Paterson Formation|70763|5|Briefly described|Map legend.|Permian|Carboniferous|Canning Basin.|||||Conglomerate (including diamictite), sandstone and siltstone; largely glacigene.|
27874|Paterson Formation|70793|4|Described|GEOL_LUT_CSV files|Sakmarian|Pennsylvanian|Of Canning Basin. Events: Point Moody Extension (300-242 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|323.1-290.1 Ma (biostrat)||||Conglomerate (including diamictite), sandstone, and siltstone; largely glacigene|
27874|Paterson Formation|70802|5|Briefly described|GEOL_LUT_CSV files|Sakmarian|Pennsylvanian|Of Gunbarrel Basin, Canning Basin. Events: Point Moody Extension (300-242 Ma). See 100k_geologyp10_lut.csv, 500k_interpgeop14_lut.csv, 250k_pre_mesozoic_interpgeop_lut.csv, 100k_interpgeop_lut.csv, 100k_geologyp14_lut.csv, 500k_interpgeop_lut.csv.|323.2-290.1 Ma (biostrat)||||Diamictite; polymict with boulders of garnet gneiss, granite, schist, and metasedimentary rocks|
27874|Paterson Formation|70826|6|Mentioned|p6 tbl 3|Early Permian|Late Carboniferous|southern Canning Basin.||||||
27874|Paterson Formation|70831|5|Briefly described|p9|||||||||
27874|Paterson Formation|70936|5|Briefly described|p59-60|Permian|Permian|Geological province: Pilbara Craton.||||Underlain by Eel Creek Formation.||
27874|Paterson Formation|71003|6|Mentioned|p59-p60|||Pilbara Craton.||||Overlies the Eel Creek Formation.|Glacial deposits.|
27874|Paterson Formation|71042|6|Mentioned|p69, p76, p79, p86|Permian|Permian|Glacial sedimentary units.||||||28-MAY-19
27874|Paterson Formation|71080|5|Briefly described|p30 fig 21|Permian|Carboniferous|Canning Basin.|||||Dominantly diamictite overlain by sandstone with some conglomerate.|
27874|Paterson Formation|71088|6|Mentioned|p32|Permian|Carboniferous||||||Pebbly sandstone, conglomerate and diamictite.|02-MAY-23
27874|Paterson Formation|71146|6|Mentioned|p38|||Southwestern Canning Basin. ||||||
27874|Paterson Formation|71169|5|Briefly described|p10, p67|Permian|Permian||||||Glacigene sedimentary rocks.|
27874|Paterson Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Poorly sorted sandstone, claystone, conglomerate, tillite, siltstone, diamictite; varves and erratics in places-glacigene, lacustrine, to fluvioglacial.|
27874|Paterson Formation|71268|4|Described|GEOL_LUT_CSV files|Sakmarian|Pennsylvanian|Of Canning Basin. Evens: Point Moody Extension (300-242 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|323.2-290.1 Ma (biostrat)||||Conglomerate (including diamictite), sandstone, and siltstone; largely glacigene|
27874|Paterson Formation|71270|4|Described|GEOL_LUT_CSV files|Cisuralian|Pennsylvanian|Of Gunbarrel Basin, Canning Basin. Events: Point Moody Extension (300 - 242 Ma). See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 100k_geologyp14_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop_lut.csv, 100k_geologysub14_lut.csv, minerie_100k_geologyp_lut.csv.|323.3-290.1 Ma (biostrat)||||Polymictic conglomerate (including diamictite), sandstone with pebbly to bouldery siltstone, conglomerate, and mudstone; probably of fluviatile origin.|
27874|Paterson Formation|71592|5|Briefly described|Appendix A.|||Canning Basin.|498+/-11 Ma (MDA: U-Pb zircon SHRIMP)||||Medium-grained, porpoius quartz-rich sandstone; diamictite.|
27874|Paterson Formation|71618|6|Mentioned|p129|Permian|Permian|Correlatable to Lower Permian diamictites in the Madura Shelf.||||||05-SEP-19
27874|Paterson Formation|71795|5|Briefly described|p34 fig 3, p43|Permian|Permian|Talbot Terrane, Rudall Province. Deposited in a paleovalley system and contains granitic boulders.|||||Tillite with granitic boulders.|
27874|Paterson Formation|71810|5|Briefly described|Map legend.|Permian|Carboniferous|Canning Basin.||||Overlies Maurice Formation.|Conglomerate (including diamictite), sandstone, and siltstone; largely glacigene (line unit in section only).|
27874|Paterson Formation|71894|6|Mentioned|p8, p12|||||||Equivalent to the Grant Group||
27874|Paterson Formation|72034|5|Briefly described|500k_interpgeop16_lut|Sakmarian|Pennsylvanian|Glacigene rocks, Canning Basin.  Age from biostratigraphy.|||||Conglomerate (including diamictite), sandstone, and siltstone; largely glacigene.|
27874|Paterson Formation|72094|5|Briefly described|p3 Fig 2, p12, 13 , 14 ,p15-16, 18|Permian|Carboniferous|Canning Basin.||||Underlain by Neoproterozoic rocks of the Officer Basin.||
27874|Paterson Formation|72499|5|Briefly described|p8|Late Mississippian|Late Mississippian|Southern marginal shelves of Canning Basin.|||||Includes glacigenic sediments.|
27874|Paterson Formation|73117|5|Briefly described|p26|||Of Traves et al. (1956). Southern lateral equivalent of the Grant Group where outcrops of the formation probably equate to a relatively high position within the group. 35 m thick. Glacial in origin. Authors suggest the use of this name for scattered outcrops of the [Grant Group equivalent] that overlie Precambrian basement, such as across the West Australian Craton and associated Proterozoic basins; whereas, the name Grant Group is most appropriate for the main part of the Canning Basin.||||Equivalent to Grant Group.|Sandstone and conglomerate.|
27874|Paterson Formation|73184|6|Mentioned|p201 Fig.12|Asselian|Asselian|Written as Paterson Fm.||||||
27874|Paterson Formation|73345|6|Mentioned|p227|||||||Equivalent to Grant Group.||
27874|Paterson Formation|73346|5|Briefly described|p2-3, p6, p28, App.1 p33|||Canning Basin. Glacigene. Earlier usage of this name applied to the relatively thin southern extensions and sections along the eastern edge of the basin; however, recent recommendations restrict the term to scattered outcrops overlying Precambrian basement on the western side of the Canning Basin around the type section and farther south, and use the more encompassing term Grant Group elsewhere. Type section is in the Paterson Range 8 km southwest of Telfer where it has a thickness of 35 m. Unconformably overlies basement at the type section.||Grant Group||||
27874|Paterson Formation|73437|6|Mentioned|p151|Paleozoic|Paleozoic|Canning Basin.||||||
27874|Paterson Formation|73453|6|Mentioned|p2|||||||||
25384|Paulsen Volcanics|35176|6|Mentioned|p13|||Petrology of volcanic rocks.||||||
25384|Paulsen Volcanics|35218|2|Defined|p16|Neoarchean|Neoarchean|Appendix 3||||||07-NOV-08
25384|Paulsen Volcanics|37327|6|Mentioned|p391|||||||||
25384|Paulsen Volcanics|72758|6|Mentioned|p5.|||Mafic volcanics of f Horwitz (1978). Name discarded. These rocks now incorporated in the Mount Roe Basalt, Fortescue Group.||||||
34414|Peak Hill Schist|12099|5|Briefly described|p676, p677-8 Figs.2 & 4, p684 Fig.8,p686|Orosirian||Previously called Peak Hill Metamorphic Suite and considered to be part of the Glengarry Group (Gee, 1987). Basement to Bryah Group. Economically important||||In tectonic contact with Bryah Group along the Goodin Fault.||04-MAR-13
34414|Peak Hill Schist|22716|6|Mentioned|p232,234|Paleoproterozoic|Paleoproterozoic|Consider together with Bryah and Padbury Group rocks to form a coherent tectono- metamorphic domain.||||||07-NOV-08
34414|Peak Hill Schist|23151|5|Briefly described|p64|||Formerly Peak Hill Metamorphic Suite. of Glengarry Group.||||||15-DEC-08
34414|Peak Hill Schist|23153|4|Described|p82,83|||||||||
34414|Peak Hill Schist|23593|5|Briefly described|p2 Fig 1|||||||||
34414|Peak Hill Schist|23597|5|Briefly described|p2 Fig 1|||||||||
34414|Peak Hill Schist|23600|5|Briefly described|p4 Fig 2|||||||||
34414|Peak Hill Schist|23744|5|Briefly described|p11|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
34414|Peak Hill Schist|23747|4|Described|p5|Archean|Archean|||||||07-NOV-08
34414|Peak Hill Schist|23748|5|Briefly described|Map Legend|Archean|Archean|||||||07-NOV-08
34414|Peak Hill Schist|23749|4|Described|p6|Archean|Archean|||||||07-NOV-08
34414|Peak Hill Schist|23750|5|Briefly described|Map Legend|Archean|Archean|||||||07-NOV-08
34414|Peak Hill Schist|23865|5|Briefly described|p170 Fig.1|||||||||
34414|Peak Hill Schist|24021|6|Mentioned|p3, Fig. 1|||||||||
34414|Peak Hill Schist|24028|5|Briefly described|p288 Fig. 1|||||||||
34414|Peak Hill Schist|49893|6|Mentioned|p2 Fig.1|||||||||
34414|Peak Hill Schist|49896|5|Briefly described|p4 Fig. 1|||Geological Province: former Glengarry Basin.||||||
34414|Peak Hill Schist|50216|6|Mentioned|p214|||Geological Province: on the margin of Bryah and Padbury Basins.||||||
34414|Peak Hill Schist|50222|6|Mentioned|p320 Fig. 3, p335|||Age: 2.67Ga.U/Pb SHRIMP zircon or monazite age.||||||13-NOV-13
34414|Peak Hill Schist|50226|5|Briefly described|p421 Fig. 4, p422-423|||Mylonitic tectonic unit.  May be part of the soutwestern tip of the Archaean Marymia Inlier (Pirajno and Occhipinti, 2000).||||||24-JUN-04
34414|Peak Hill Schist|61271|6|Mentioned|p105 Fig.1|||||||||
34414|Peak Hill Schist|61848|6|Mentioned|p301, p303|||||||||
34414|Peak Hill Schist|62289|5|Briefly described|plate 1, p2, p3 Fig. 1|Palaeoproterozoic|Archean|Marymia Inlier, Yilgarn Craton; quartz-muscovite schist, mylonitic schist, and phyllonite.||||||23-OCT-15
34414|Peak Hill Schist|64580|4|Described|map legend|Proterozoic|Archean|Quartz muscovite schist, mylonitic schist, and phyllonite.||||||15-DEC-08
34414|Peak Hill Schist|64725|5|Briefly described|p64.|||A mylonitic tectonic unit with Au and Au-Cu lode deposits.||||||
34414|Peak Hill Schist|65408|6|Mentioned|p81, p84 Fig.1.|Archean|Archean|Formerly the Peak Hill Metamorphics. Part of Marymia Inlier.||||||
34414|Peak Hill Schist|65411|6|Mentioned|p89 Fig.1.|Archean|Archean|||||||
34414|Peak Hill Schist|65412|6|Mentioned|p97 Fig.1.|||||||||
34414|Peak Hill Schist|65419|1|Redefined|p2, p4 Fig.1, pp3-6, p8, p27.|Paleoproterozoic|Paleoproterozoic|Originally, in part Peak Hill Beds (MacLeod 1970); later Peak Hill Metamorphic Suite (Gee 1979) then Peak Hill Metamorphics (Gee 1990); transferred to the Glengarry Group by Gee and Grey (1993). Subsequently renamed Peak Hill Formation, in the Bryah Group, (Pirajno and Occhipinti 1995). Separated, renamed and revised in this study to consist of Gee's (1979) Peak Hill Metamorphic Suite, minor metabasite, and the northern part of the Doolgunna Arkose as shown by Gee (1987). No type section; type area is 'within a 7 km radius of the Peak Hill townsite' (Gee, 1979). Age is unknown. Called Peak Hill Schists on p8.|||Includes Crispin Mylonite.|In faulted contact with Bryah Group and Juderina Formation.|Mylonitic schist, phyllonite, quartz-muscovite schist, quartz-sericite schist, quartz blasto-mylonite, calc-silicate schist, minor metabasite schist; predominantly greenschist facies.|
34414|Peak Hill Schist|65913|6|Mentioned|p2 Fig.1. |||||||||
34414|Peak Hill Schist|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv|Proterozoic|Archean||||||Quartz muscovite schist, mylonitic schist, and phyllonite|
34414|Peak Hill Schist|69003|6|Mentioned|p11|Archean|Archean|A mylonitized part of the Marymia Inlier. Hosts orogenic, shear zone-hosted gold lodes.||||||
34414|Peak Hill Schist|69166|5|Briefly described|500k_geologyp08_lut.csv|Proterozoic|Archean||||||Quartz muscovite schist, mylonitic schist, and phyllonite.|
34414|Peak Hill Schist|69596|6|Mentioned|p4|Archean|Archean|Capricorn Orogen.||||||
34414|Peak Hill Schist|70795|5|Briefly described|2_5m_interpgeop15_lut.csv|Paleoproterozoic|Mesoarchean|Also 500k_interpgeop14_lut.csv|3131-1600 Ma||||Quartz muscovite schist, mylonitic schist and phyllonite.|
34414|Peak Hill Schist|70796|4|Described|2_5m_interpgeop15_lut.csv|Paleoproterozoic|Mesoarchean|Capricorn Orogen. Affected by the following events: Mulka Tectonic Event (570  570 Ma); Edmundian Orogeny D3e/M3e (995  954 Ma); Edmundian Orogeny (1026  954 Ma); Edmundian Orogeny D1e/M1e (1026  995 Ma); Edmundian Orogeny D2e/M2e (1026  995 Ma); Mutherbukin Tectonic Event (1321  1171 Ma); Mangaroon. See also 500k_interpgeop14_lut.csv.|ca. 3131 to 1600 ma (inferred)||||Quartz muscovite schist, mylonitic schist, and phyllonite|
34414|Peak Hill Schist|70804|4|Described|p1-p2, p4-p6, p17, p23|Archean|Archean|Replaces the Peak Hill Metamorphic Suite which was previously assinged to the Glengarry Group. Exposed in the 'Peak Hill Dome'. Hosts the Peak Hill, Jubilee and Mount Pleasant gold deposits. See also p25-p26, p28-p30, p32, p38, p40-p41, p43, plate 1.||||Faulted against the Bryah Group.|Phyllonite, quartz-muscovite schist, calc-silicate schist, sericite schist and quartz-muscovite-biotite-chlorite schist.|
34414|Peak Hill Schist|70826|6|Mentioned|p9|Neoarchean|Neoarchean|Large uncertainty in age constraints, and possible correlation with greenstones in Marymia Inlier. May be part of younger sedimentary succession. Strongly affected by deformation within Capricorn Orogen.||||||
34414|Peak Hill Schist|71000|6|Mentioned|p65|||Marymia Inlier, southern Gascoyne Province, Capricorn Orogen. Contains orogenic gold.||||||
34414|Peak Hill Schist|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||pelite, calc-silicate rock, greenstone|
34414|Peak Hill Schist|71269|5|Briefly described|GEOL_LUT_CSV files|Paleoproterozoic|Mesoarchean|Geological province: Capricorn Orogen, Yilgarn Craton. Of Marymia Inlier. Events: Mulka Tectonic Event (570-570 Ma); Edmundian Orogeny D3e/M3e (995-954 Ma); Edmundian Orogeny (1026-954 Ma); Edmundian Orogeny D1e/M1e (1026-995 Ma); Edmundian Orogeny D2e/M2e (1026-995 Ma); Mutherbukin Tectonic Event (1321-1171 Ma); Mangaroon ??. See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv.|3131-1600 Ma (inferred)||||Quartz muscovite schist, mylonitic schist, and phyllonite|
34414|Peak Hill Schist|71468|6|Mentioned|p24|||Geological province: Capricorn Orogen, Yilgarn Craton.||||||
34414|Peak Hill Schist|71484|4|Described|p122-126,133-135,137,139|||Of greenschist to amphibolite metamorphic facies. Includes mica fish in quartz blastomylonite, consistent with high strain deformation (Occhipinti et al., 1998). Protoliths were likely siliciclastic sedimentary succession with minor interbedded calcareous and chemical sedimentary rock. Deformed during c. 1960 Ma Glenburgh Orogeny?|||Includes Crispin Conglomerate.||Quartz blastomylonite, quartz-muscovite mylonite, quartz-muscovite schist, quartz-muscovite-biotite-albite-(chlorite) schist, with minor amphibolite, calc-silicate schist and quartz-magnetite-garnet mylonite.|30-AUG-19
34414|Peak Hill Schist|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Mesoarchean|Capricorn Orogen.|||||Quartz muscovite schist, mylonitic schist, and phyllonite.|
40841|Pear Creek Formation|63420|5|Briefly described|Map legend|Archean|Archean|Of Fortescue Group (Mount Bruce Supergroup). Geological Province: Marble Bar Sub-basin/Hamersley Basin. Polymictic conglomerate, matrix-supported clasts of Fortescue Group basalt and older chert, felsic rock and granitic rock.||||||07-NOV-08
40841|Pear Creek Formation|64326|3|Fully described|p73-77|Archean|Archean|Of Fortescue Gp. Overlies Kylena Fm in Pear Creek Centrocline only (Hamersley Basin) - elsewhere unit overlain by Tumbiana Fm. Comprises 5 units: sst/siltst, sst, pebbly sst/conglom.+quartzose sst/conglom (detailed lith.given). Combined thickness: >1080m.||||||15-APR-13
40841|Pear Creek Formation|64621|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Fortescue Group. Polymictic and oligomictic conglomerates containing clasts and cobbles of Fortescue Group basalts; medium- to coarse-grained sandstone; local beds of pebble conglomerate; some basalt, fine-grained.||||||07-NOV-08
40841|Pear Creek Formation|64936|5|Briefly described|map legend|Archean|Archean|Of Fortescue Group, Mount Bruce Supergroup. Over Kylena Formation. Conglomerate, sandstone, breccia, siltstone; with clasts of Fortescue Group basalt, basement chert, felsic volcanic rock, and granite. Geol. Prov: Hamersley Basin, Pilbara Craton.||||||
40841|Pear Creek Formation|66108|5|Briefly described|Map legend|Neoarchean|Neoarchean|Unit in Fortescue Group. Conglomerate and other siliciclastic rocks interlayered with basalt; clasts range from boulders to pebbles; dominantly basaltic clasts; granitic, felsic volcanic, and chert clasts present locally.||||||
40841|Pear Creek Formation|66217|4|Described|p5, p6 Table 1, pp48-54.|Neoarchean|Neoarchean|Fortescue Basin, Pilbara Craton. Thickness to 1 km. Equivalent to Pear Creek Sequence of Blake (1993). Deformation (growth faulting) occurred during deposition.|<2740 Ma.|Unit in Fortescue Group.||Unconformably overlies the Kylena Formation.|Brown-to-green-weathering, well-preserved clastic sedimentary rocks: interbedded sandstone and conglomerate, and basaltic breccia.|
40841|Pear Creek Formation|68283|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Marble Bar Sub-basin, Fortescue Basin.||Of the Fortescue Group.|||Polymictic conglomerate; matrix-supported clasts of Fortescue Group basalt and older chert, felsic volcanic rock, and granitic rock.|07-JAN-15
40841|Pear Creek Formation|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Fortescue Group|||Polymictic conglomerate, oligomictic conglomerate, boulder conglomerate, older chert and breccia, felsic volcanic rocks and granitic rocks. Quartz arenite and quartz rich sandstone, siltstone and local beds of pebble conglomerate.|
40841|Pear Creek Formation|69590|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Of Marble Bar Sub-basin, Fortescue Basin. Events: Pilbara Craton breakup. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|2735-2629 Ma (inferred)|Unit of Fortescue Group.|||Basalt, medium- to coarse-grained sandstone; oligomictic to polymictic boulder conglomerate with interbeds of quartz arenite and quartz-rich sandstone, partly volcaniclastic siltstone.|
40841|Pear Creek Formation|70795|6|Mentioned|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean||2735-2629 Ma|||||
40841|Pear Creek Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone, basalt|
40841|Pear Creek Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Marble Bar Sub-basin, Fortescue Basin.|Max age 2735+/-5 Ma, min ~2713 Ma.|Fortescue Group, sequence 4|||Conglomerate and other siliciclastic rocks interlayered with basalt; clasts range from boulders to pebbles; dominantly basaltic clasts; granitic, felsic volcanic, and chert clasts present locally.|
74047|Pearce Formation|13222|6|Mentioned|p229 Fig.2.|||||Unit in Kinmore Group.||||
74047|Pearce Formation|13242|2|Defined|p214 Fig. 2, p215|Late Permian|Late Permian|Supersedes Pearce Mbr (Hyland Bay Fm). Now in Hyland Bay Sub-group (Kinmore Gp). Unconf. under Cape Hay Fm. Geol. Prov: Bonaparte Basin.Three lithological units - Lower + Upper Pearce Fm (in 'defined' format) + possible lower member, Torrens Mbr (informal). Type section in Petrel 2, 3952-3983 m.|||||Two limestones separated by a clastic unit, usually shale|21-DEC-12
74047|Pearce Formation|60386|6|Mentioned|p297|||Bonaparte Basin/Petrel Sub-basin.  Limestone nearshore-shelf.||||||
74047|Pearce Formation|61542|6|Mentioned|p284 Fig. 10|||||||||07-FEB-11
74047|Pearce Formation|64630|5|Briefly described|p31 Fig.2|Wordian|Wordian|Province: Bonaparte Basin. Unconformably underlies the Cape Hay Formation, overlies the Fossil Head Formation. Palynology age: D. ericianus to P. rugatus.||||||11-JAN-10
74047|Pearce Formation|64690|6|Mentioned|p503, p504 Fig.2|Late Permian|Late Permian|||Unit in Hyland Bay Sub-group.||Overlies Fossil Head Formation. Is overlain by Cape Hay Formation.|Carbonates.|
74047|Pearce Formation|64692|6|Mentioned|p522 Fig.2 |Late Permian|Late Permian|Bonaparte Basin.||Unit in Hyland Bay Sub-group.||Is overlain by Cape Hay Formation.||
74047|Pearce Formation|67354|5|Briefly described|p102 Fig.33.|Wordian|Wordian|||||Overlies Torrens Formation.||
74047|Pearce Formation|67370|6|Mentioned|p314 Fig.3, p316 Fig.5. |Permian|Permian|||Unit in Hyland Bay Subgroup.||Overlies Torrens Formation. Is overlain by Cape Hay Formation.||
74047|Pearce Formation|69452|4|Described|p36:8, 15, 19-20|Capitanian|Kungurian|Gorter (1998); formerly Pearce Member of Hyland Bay Formation (Mory, 1988). Petrel Sub-basin, Bonaparte Basin. Offshore marine to marine shelf deposits. Up to 50m thick. Offshore and onshore.||Hyland Bay Subgroup.||Unconformably overlies Fossil Head Formation. Is overlain unconformably by Cape Hay Formation.|A lower unit of bioclastic limestone with abundant bryozoans and minor shelly debris, increasingly dominated by clastic rocks; upper unit of dark shale overlain by allochthonous bioclastic limestone with brachiopods, bryozoans and shelly debris.|12-JUL-16
74047|Pearce Formation|69454|5|Briefly described|p38:4|Capitanian|Wordian|Petrel Sub-basin, Bonaparte Basin.||Hyland Bay Subgroup.||||12-JUL-16
74047|Pearce Formation|69653|6|Mentioned|p10|Guadalupian|Guadalupian|Petrel Sub-basin.||Hyland Bay Sub-group.||Overlies Torrens Formation. Is overlain by Cape Hay Formation.||
74047|Pearce Formation|69673|6|Mentioned|p153 fig 125, p173|||||Hyland Bay Subgroup||Overlain by Cape Hay Formation, overlies Torrens Formation||
74047|Pearce Formation|70061|5|Briefly described|Petrel Sub-basin Figs.2 & 3|Capitanian|Wordian|See also Regional geology: Figs.6-8, p11. Vulcan: Fig.2. Shoreface to open marine biomicritic limestones form an intraformational seal.||Hyland Bay Subgroup.||Overlies Torrens Formation. Is overlain by Cape Hay Formation.||12-JUL-16
74047|Pearce Formation|70774|5|Briefly described|p5 fig 3|Kazanian|Kazanian|Bonaparte Basin.||||||
74047|Pearce Formation|71623|4|Described|p344, 346, 347, 355, 358, 359, 346||Roadian|In Timor Sea region, at Petrel Field, Tern Field. Part of Pearce Cycle. Marine. See also p343 and p349.||||Correlated with Beekeeper and Cody Formations|Upper bioclastic limestone, middle shale and siltstone, lower interval of two thinner bioclastic limestones separated by shale at Petrel field. Calcareous sandstone at base in Tern field.|08-MAY-19
27535|Pedestal beds|23621|4|Described|p36|Devonian|Devonian|See also Page 9 Table 1. Underlain by Gardiner Sandstone. In the Ord Basin. Max. thickness: >10 m.||||||22-NOV-06
27535|Pedestal beds|23622|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Ord Basin.||||||
27535|Pedestal beds|36335|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
27535|Pedestal beds|43301|6|Mentioned|Map Legend||Paleozoic|age Devonian?||||||07-NOV-08
27535|Pedestal beds|43631|6|Mentioned|p27|||||||||
27535|Pedestal beds|45155|6|Mentioned|p42|||||||||
27535|Pedestal beds|61861|5|Briefly described|p4|Devonian|Devonian|Flat-lying siliciclastic rocks. Also mis-spelt as Pedestal Beds on same page.||||Overlies Antrim Plateau Volcanics, unconformably overlies Dead Bullock Formation.||03-APR-12
27535|Pedestal beds|62632|5|Briefly described|Map Legend|Paleozoic|Paleozoic|Sandstone, fine grained, planar bedded, laminated; conglomeratic sandstone, laminated, silicified, ferruginous; conglomerate.||||||07-NOV-08
27535|Pedestal beds|64675|6|Mentioned|p10|||See also Pedestal Beds||||||
27535|Pedestal beds|65074|4|Described|p350 fig 4-36, p351, p358-360, p362|Devonian|Devonian|Of North/Centre Birrindudu Basin. Appears as Pedestal Beds on p350. 500 m thick. Type area is in Macfarlanes Peak Range (NT). Non-fossiliferous.||||Possibly equivalent to Pertnjara Group (NT). Overlies (all unconformably) Lucas Formation, Tanami Complex, Redcliff Pound Group, Hidden Basin beds, Antrim Plateau Volcanics.|Quartz sandstone; minor conglomerate, shale, siltstone.|
27535|Pedestal beds|67163|5|Briefly described|Map legend.|Paleozoic|Paleozoic|||||Overlies Lucas beds.|Sandstone, fine-grained, planar-bedded, laminated; conglomeratic sandstone, laminated, silicified, ferruginous; conglomerate, well-rounded cobbles and pebbles, thickly bedded, graded.|19-OCT-11
27535|Pedestal beds|69288|5|Briefly described|Map legend.|Paleozoic|Paleozoic|Also appears as Pedestal Beds.|||||Fine-grained, planar-bedded, laminated sandstone; laminated, silicified, ferruginous conglomeratic sandstone with beds 30cm - 1m thick; thickly-bedded, graded conglomerate with well rounded cobbles and pebbles.|
27535|Pedestal beds|69440|5|Briefly described|p25:2|Devonian|Devonian|Canning Basin.||||Unconformably overlies Erica Sandstone.||12-JUL-16
27535|Pedestal beds|69453|5|Briefly described|p37:1-2|||Lucas Outlier, Canning Basin. Up to 500m thick. Deformation (including E-plunging folds) occurred probably during the Alice Springs Orogeny.||||Unconformably overlies Antrim Plateau Volcanics; inferred to unconformably overlie Lucas Formation. Stratigraphically equivalent to Pertnjara Group.|Medium- to fine-grained, poorly sorted, thin to very thick quartz sandstone with isolated (stringers of) pebbles; interbedded with minor massive, pebble and cobble conglomerate, and shale.|12-JUL-16
27535|Pedestal beds|69673|5|Briefly described|p200|||Up to 500m thick.|||||Thin to very thick sandstone interbedded with minor conglomerate and shale.|
27535|Pedestal beds|70852|5|Briefly described|Map legend.|Paleozoic|Paleozoic|Canning Basin.|||||Quartz sandstone; minor conglomerate, siltstone, shale.|
27535|Pedestal beds|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Fine grained sandstone, planar bedded, laminated; conglomeratic sandstone with beds 30 cm-1 m;laminated, silicified, ferruginous; conglomerate, well rounded cobbles and pebbles, thickly bedded, graded.|
74168|Pegasus Dolomite Member|64643|5|Briefly described|p3 Fig. 2|Llandovery|Llandovery|Of Sahara Formation?||||||
74168|Pegasus Dolomite Member|65449|3|Fully described|p1, p6, p8, p10, p19-21, p23, p28-29,p40|Llandovery|Llandovery|See also p47-50, p59; Plates 1-9, 11. New name, after Pegasus 1 petroleum well. A dolomite horizon inferred by Lehmann (1984) to mark the base of the Mount Troy Formation in Barbwire 1; reinterpreted in this Report. Type section is the interval 552.6-550.45m in Acacia 1; a reference locality for western areas is the interval 975.5-971.75m in mineral exploration drillhole Brooke 1. Maximum thickness of 5m in Mirbelia 1 (p29), or 4.5m in Pegasus 1, Sally May 1 (defn p59) ; 2.15m at type section. Only known from sub-surface. A useful marker to identify the Sahara Formation, particularly where the Mallowa Salt is absent. Has a distinctive signature on wireline logs. Formed during a brief basin-wide marine incursion. Lies 20-40m below the base of the Worral Formation. No fossils known; age from surrounding units.||Of Sahara Formation.|||Light-grey, hard, massive dolomite, stylolitic, with infilled subvertical fractures, microfaults, calcite filled veins, and minor vuggy porosity; argillaceous to silty dolomite.|24-FEB-20
74168|Pegasus Dolomite Member|68007|5|Briefly described|p11, Plate 1|||May be the 1m-thick unit producing a 'mirror image' spike on back-to-back gamma ray and sonic logs.||Of Sahara Formation.|||A thin carbonate unit.|24-FEB-20
74044|Penguin Formation|13222|6|Mentioned|p229.|Late Permian|Late Permian||||||Sandstone.|
74044|Penguin Formation|13242|2|Defined|p214 Fig. 2, p223|Late Permian|Late Permian|Of Hyland Bay Sub-group. Unconformable over Tern Fm; passes upwards conformably up into Mount Goodwin Formation. Lithology varies - claystone, siltstone and sandstone (detailed lithology included). Geol. Province: Bonaparte Basin.  See also p226 Fig. 8.||||||07-FEB-11
74044|Penguin Formation|64690|5|Briefly described|p504 Fig.2 |Late Permian|Late Permian|||Unit in Hyland Bay Sub-group.||Overlies Tern Formation. Is overlain by Lower Mount Goodwin Formation.||
74044|Penguin Formation|64692|6|Mentioned|p522 Fig.2 |Late Permian|Late Permian|Bonaparte Basin.||Unit in Hyland Bay Sub-group.||Overlies Tern Formation. Is overlain by Lower Mount Goodwin Formation.||
74044|Penguin Formation|67370|3|Fully described|pp313-317. |Changhsingian|Changhsingian|Of Gorter (1998). Bonaparte Basin. Type section in Tern-3 between 2,400 - 2,449 m. Occurs in some wells between the undoubtedly Late Permian Tern Formation and the well-dated basal Triassic. Contains the P. microcorpus Oppel Zone at Fishburn-1. The base of this unit is an unconformity overlying older Permian strata. The top of this unit marks the base of the Triassic. Few spinose acritarchs; little if any bioturbation: possibly an oxygen-poor lacustrine facies. Granite clasts in the pebble lag layer suggest long distance transport from granitic terrain to the south.||Basal unit in Mount Goodwin Subgroup.||Unconformably overlies Tern, Cape Hay and Dombey Formations. Is overlain conformably by Mairmull Formation.|Medium-grey to dark grey-brown claystone; finely laminated shales; local pebble lag.|
74044|Penguin Formation|69452|4|Described|p36:8, 15, 20-21|Changhsingian|Changhsingian|Petrel Sub-basin, Bonaparte Basin. Offshore. Up to 49m thick in the type section in drillhole Tern-3.||Mount Goodwin Subgroup.||Unconformably overlies Hyland Bay Subgroup. Is overlain conformably by Mairmull Formation.|Claystone, carbonaceous siltstone and minor calcareous sandstone in upward-coarsening cycles.|12-JUL-16
74044|Penguin Formation|69454|5|Briefly described|p38:4|Changhsingian|Changhsingian|Petrel Sub-basin, Bonaparte Basin.||Mount Goodwin Subgroup.||||12-JUL-16
74044|Penguin Formation|69653|6|Mentioned|p10|Changhsingian|Changhsingian|Petrel Sub-basin.||Hyland Bay Sub-group.||Overlies Tern Formation. Is overlain by Mairmull Formation.||
74044|Penguin Formation|69673|6|Mentioned|p153 fig 125|||||Mount Goodwin Subgroup||Overlain by Mairmull Formation, overlies Tern Formation||
74044|Penguin Formation|70061|5|Briefly described|Petrel Sub-basin Figs.2 & 3, p2|Induan|Induan|See also Regional geology: Figs.6-8, p10. Vulcan: Fig.2. Hydrocarbon reservoir, especially gas at Fishburn 1.||Mount Goodwin Subgroup.||Overlies Tern Formation. Is overlain by Mairmull Formation.||12-JUL-16
74044|Penguin Formation|70774|5|Briefly described|p5 fig 3|Dorashamian|Dorashamian|Bonaparte Basin. [old age name terminology used]||||||04-JAN-18
74044|Penguin Formation|71623|5|Briefly described|p355, 359, p345 fig 2, p346,347,352,353|Changhsingian|Changhsingian|Bonaparte Basin. Sonic logs shown in figures.|||||Sandstone|
74044|Penguin Formation|72505|5|Briefly described|p890|Induan|Induan|Southern Bonaparte Basin. Correlated to the P. microcorpus zone.||||Overlies the Tern Formation.||
74044|Penguin Formation|73304|6|Mentioned|p71, p77|||Bonaparte Basin. Contains the late Changhsingian mass extinction level.||||||
26838|Penneshaw Formation|22682|6|Mentioned|p12||Archean|Same as Noganyer Formation. Also see Fig9, p14||||||07-NOV-08
26838|Penneshaw Formation|23136|6|Mentioned|p265 Fig.1|||||||||
26838|Penneshaw Formation|23159|5|Briefly described|fig4 p804|Archean|Archean|||||||07-NOV-08
26838|Penneshaw Formation|23926|5|Briefly described|p9|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
26838|Penneshaw Formation|30562|4|Described|p8|||See also p7. Archaean age||||||18-MAY-21
26838|Penneshaw Formation|30959|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
26838|Penneshaw Formation|31093|6|Mentioned|Fig. 4|||||||||
26838|Penneshaw Formation|36869|6|Mentioned|p48|||||||||
26838|Penneshaw Formation|41432|5|Briefly described|p12|||||||||
26838|Penneshaw Formation|42195|5|Briefly described|p143|||||||||
26838|Penneshaw Formation|42221|4|Described|p32|||||||||
26838|Penneshaw Formation|42937|5|Briefly described|p559|||||||||
26838|Penneshaw Formation|43052|5|Briefly described|Fig.3.8|||||||||
26838|Penneshaw Formation|43102|5|Briefly described|p11|||||||||
26838|Penneshaw Formation|43162|6|Mentioned|6|||U-Pb age: 2938+/-10Ma||||||
26838|Penneshaw Formation|43496|6|Mentioned|15|||Age: 2900Ma||||||
26838|Penneshaw Formation|43498|5|Briefly described|2|||U-Pb SHRIMP Age: 2.9 Ga and 3.1 Ga||||||18-MAY-21
26838|Penneshaw Formation|60076|4|Described|p14-15, p16 Fig. 6|Archean|Archean|Mainly amphibolites and massive to pillowed basalts, with minor felsic volcanic and sedimentary rocks; also contains porphyritic felsic schists with amphibolite intervals.  Overlain by Noganyer Formation.  Age: 2930+/-4Ma and 2938+/-10Ma.||||||07-NOV-08
26838|Penneshaw Formation|64161|5|Briefly described|p581|||<2930 Ma. Of Eastern Goldfields Superterrane||||||
26838|Penneshaw Formation|64633|6|Mentioned|p6 Fig.4.|||Kalgoorlie Terrane, Norseman Domain.|||||Lower part: basalt, often pillowed; upper part: sedimentary rocks, mainly fine-grained turbidites.|
26838|Penneshaw Formation|65264|5|Briefly described|p11|Archean|Archean|Age: 2930+/-4Ma (for rhyolite), 2938+/-10Ma (Campbell and Hill 1988). Geological province: Norseman terrane. Consists mainly of amphibolites and massive to pillowed basalts, with minor felsic volcanic rocks.||||||07-FEB-11
26838|Penneshaw Formation|67198|5|Briefly described|p4|||Doepel (1973); McGoldrick (1993). Eastern Norseman Domain, Kalgoorlie Terrane.|c.2.9 Ga.|||||
26838|Penneshaw Formation|68107|5|Briefly described|p618, p619 Fig.8|Mesoarchean|Mesoarchean|Southern Kalgoorlie Terrane. May represent a basement fragment underlying the <2720 Ma Kambalda Sequence.|ca. 2930 Ma (Nelson 1997).|||Overlain by the Kambalda Sequence ?||
26838|Penneshaw Formation|69152|5|Briefly described|geochron file 104963.1.pdf|Mesoarchean|Mesoarchean|Geochron file 104963.1.pdf describes dating of felsic volcanic within this unit. Age of deposition: 2930+/-4 Ma. (published 1997?)||||||
26838|Penneshaw Formation|69404|6|Mentioned|p4 Fig.4|Mesoarchean|Mesoarchean|Kalgoorlie Terrane.|c. 2950 Ma|||||
26838|Penneshaw Formation|69617|6|Mentioned|p155|||Norseman area, Eastern Goldfields Superterrane.||||||
26838|Penneshaw Formation|70153|5|Briefly described|104963.1.pdf|Archean|Archean|Age derived from sample of metamorphosed rhyolitic lapilli tuff (104963.1.pdf)|2930 Ma +/- 4 Ma (SHRIMP)||||Includes biotite rhyolite.|
26838|Penneshaw Formation|70802|5|Briefly described|104863.1.pdf|Mesoarchean|Mesoarchean|Sample GSWA 104863 (rhyolite) yielded a 207Pb/206Pb age of 2930+\4 Ma, interpreted to be depositional age of the rhyolite.|2930+\-4 Ma|||||
26838|Penneshaw Formation|71270|5|Briefly described|104963.1.pdf|Mesoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Zircon analysis conducted on sample GSWA 104963 (biotite rhyolite) yielded an interpreted depositional age of 2930+\-4 Ma.|2930+\-4 Ma.|||||
26838|Penneshaw Formation|72049|5|Briefly described|p255, p259|||Kalgoorlie Terrane. Informally subdivided into an upper and lower unit on p259.|2930 +/- 4 Ma (Nelson, 1995)||||Felsic volcanic rocks.|
26838|Penneshaw Formation|73391|5|Briefly described|p303, 435-436, 445|Archaean|Archaean|Swager et al. (1990). Norseman Terrane; southern end of the Eastern Goldfields Province. Oldest greenstones in the Eastern Goldfields Province.|2938 +/- 10 Ma (Hill et al., 1992).||||Mafic volcanic rocks.|
26838|Penneshaw Formation|73596|6|Mentioned|p1165, 1170|Neoarchean|Neoarchean|Norseman Inlier, Kalgoorlie-Kurnalpi Rift.|2930 +/- 4 Ma (Nelson, 1995).||||Biotite-rhyolite, rhyolite lapilli tuff, rhyolite.|
38641|Penny Dam Conglomerate|23786|5|Briefly described|p5|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
38641|Penny Dam Conglomerate|60555|5|Briefly described|p2 Fig. 1, p5 p7, p8 Tb. 2, p12|Archean|Archean|Age: <2671+/-3Ma, range c. 2700-2650Ma. Polymictic clast-supported conglomerates, sandstones and mudstones. Submarine fan.||||||30-NOV-09
38641|Penny Dam Conglomerate|64340|6|Mentioned|p2 Fig. 1|||||||||
38641|Penny Dam Conglomerate|64633|6|Mentioned|p6 Fig.4.|||Kurnalpi Terrane.|<2671 +/- 3 Ma.|||||
38641|Penny Dam Conglomerate|64775|6|Mentioned|p8|||||||Overlies Mount Belches Formation.||30-MAR-12
38641|Penny Dam Conglomerate|65264|5|Briefly described|p21|||Geological province: Gindalbie terrane. Thought to be equivalent to Mount Belches Formation (Swager 1995a, and Krapez ert al 2000).||||||07-FEB-11
38641|Penny Dam Conglomerate|66880|6|Mentioned|p8 Fig.2. |Archean|Archean||2671 +/- 3 Ma (Krapez et al. 2000).|||||
38641|Penny Dam Conglomerate|71270|5|Briefly described|183145.1.pdf|||Geological province: Yilgarn Craton, West Australian Craton. Krapex et al., (2000) reported a maximum depositional age of 2671+\-3 Ma.||||||
38641|Penny Dam Conglomerate|72049|5|Briefly described|p256, p268|||Kurnalpi Terrane. Geochronology analyses, results, and interpretation are discussed in detail.|2671 +/- 3 Ma (SHRIMP U-Pb)|Early Merougil Group||||
38641|Penny Dam Conglomerate|73391|5|Briefly described|p284-286, 334|||Swager (1994). Yindarlgooda Dome area, eastern Kalgoorlie Terrane. SHRIMP ages by Krapez et al. (2000) and Krapez and Pickard (2010), for lower and upper units respectively. Appears as Penny Dam formation on p334.|2672 +/- 3 Ma and 2669 +/- 4 Ma.||||A sequence of clastic sedimentary rocks; a lower mafic-volcanic-clast dominated conglomerate, and an upper quartz-rich sandstone and polymictic granite-clast conglomerate.|
81323|Penzance Supersuite|70020|6|Mentioned|p122, 131|||Exposed near the Jungle Pool base metal occurrence.|c. 2680 Ma|||||07-AUG-19
81323|Penzance Supersuite|71148|6|Mentioned|p122|Neoarchean|Neoarchean|Eastern Goldfields Superterrane.|||||HFSE-enriched granites.|
81323|Penzance Supersuite|73631|5|Briefly described|p2|Archean|Archean||||Kent Complex.||HFSE-enriched granites with biotite and/or amphibole, quartz and feldspar.|
28917|Peppermint Grove Limestone|22552|6|Mentioned|p 41|||||||||
28917|Peppermint Grove Limestone|24410|5|Briefly described|p39|Quaternary|Quaternary|Of the Kwinana Group. Geological Province: Perth Basin.||||||
28917|Peppermint Grove Limestone|35097|6|Mentioned|p27|||||||||
28917|Peppermint Grove Limestone|36293|3|Fully described|p213|||||||||
28917|Peppermint Grove Limestone|40400|6|Mentioned|p109|||Of Passmore (1970). Geological Province: Perth Basin.||||||06-AUG-07
28917|Peppermint Grove Limestone|44144|4|Described|p501 Tb.4-21|Holocene|Holocene|Type Section: Peppermint Grove 31o59'30''S 115o46'10''E. 5m thickness of shallow marine estuary deposits with abundant foraminifera and molluscs.||Kwinana Group||Interfingers with Tamala Limestone.|Calcarenite and calcirudite.|
31963|Peringee Bore Granite|24197|6|Mentioned|p71 Tb. 7.1|||Of the Chararoo Supersuite.||||||07-FEB-11
31963|Peringee Bore Granite|50425|5|Briefly described|p1.3, 3.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Province. Of the Chararoo Supersuite. I-Type.||||||07-NOV-08
23899|Perkolilli Shale|22769|5|Briefly described|Table1p759||Late Eocene|||||||
23899|Perkolilli Shale|23797|5|Briefly described|p3|||Overlies Wollubar Sandstone (conformable). Geological Province: Yilgarn Craton.||||||17-FEB-05
23899|Perkolilli Shale|23989|5|Briefly described|p51|Late Eocene|Late Eocene|See also page 52. Geological Province: Yilgarn Craton||||||
23899|Perkolilli Shale|24160|5|Briefly described|p117.|||Hosts kaolin deposits in palaeochannels.||||Conformably overlies Wollubar Sandstone. Correlates with Pallinup Siltstone and lower Eundynie Group.||
23899|Perkolilli Shale|24397|5|Briefly described|p241|||Name abandoned.  Geological Province: Eucla Basin.||||||
23899|Perkolilli Shale|42535|3|Fully described|p17||late Eocene|||||||11-JUN-15
23899|Perkolilli Shale|43065|2|Defined|p89|Late Eocene||||||||
23899|Perkolilli Shale|43279|6|Mentioned|Map Legend||Tertiary|||||||
23899|Perkolilli Shale|43280|6|Mentioned|Map Legend||Tertiary|||||||
23899|Perkolilli Shale|43623|5|Briefly described|p4|||||||||
23899|Perkolilli Shale|43838|5|Briefly described|p4, 8||Tertiary|Occurs in Roe Palaeodrainage.||||||12-JUL-16
23899|Perkolilli Shale|61197|5|Briefly described|p473-474|Miocene|Oligocene|A clay-rich paludal unit in-filling inset-valleys cut into Precambrian basement.||||Unconformably overlies Wollubar Sandstone.|Clay, silt, with gravel lenses.|
23899|Perkolilli Shale|61814|5|Briefly described|p23|||Comprises thick beds of massive kaolinite and smectite, with ferruginous, siliceous and calcareous overprints, and lenses of cross-stratified ferruginous gravel.||||||08-FEB-10
23899|Perkolilli Shale|61849|6|Mentioned|p315|||||||||
23899|Perkolilli Shale|65194|5|Briefly described|p16, p137, p140-144, p157 Fig.4.50|Miocene|Oligocene|Upper unit in Roe Palaeovalley; overlies Wollubar Sandstone unconformably.  Is called Perkolilli Clay on p143. Max thickness 39m. Lacustrine. Widespread in the Yilgarn. Age discussed p142 & considered post-Eocene.|||||Mottled, grey, dark-brown and yellow clay with minor sandy clay interbeds.|08-APR-16
23899|Perkolilli Shale|65204|6|Mentioned|p22|||Clay with subordinate sandy clay.||||||
23899|Perkolilli Shale|65262|5|Briefly described|p4, p5, p6 Fig.2, p8|||Yilgarn Craton. Up to 30m thick. The unit becomes more sandy in the upper parts of the palaeochannels, and is occasionally silicified or calcretised. Relatively impermeable.||||Overlies Wollubar Sandstone.|A multicoloured clay with minor sandy clay beds.|
26841|Pernatty Dolerite|22596|6|Mentioned|Table 1 p409|Archean|Archean|||||||07-NOV-08
26841|Pernatty Dolerite|42696|6|Mentioned|Plate 1B|Archean||Presumably not related to Pernatty Quartzite, SA.||||||07-NOV-08
26841|Pernatty Dolerite|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
26841|Pernatty Dolerite|42870|5|Briefly described|Table 1, P67|||||||||
26841|Pernatty Dolerite|43102|5|Briefly described|Fig.3|||||||||
26841|Pernatty Dolerite|62108|5|Briefly described|p1409 Tb. 10|||Of the Kalgoorlie Group. Max. thickness: 500m. Geological Province: Yilgarn Craton (Boulder-Lefroy Shear Zone).||||||07-FEB-11
26841|Pernatty Dolerite|65834|6|Mentioned|p62|||New Celebration area, c.35km SE of Kalgoorlie.||||||
26841|Pernatty Dolerite|69619|5|Briefly described|p118-122, p124 Fig.8, p127, p133|||Constitutes the western (hanging) wall of the Hampden-Boulder-Jubilee gold mine. 200-600m thick. Alteration and mineralisation styles detailed.||||Equivalent to Williamstown Dolerite (Kalgoorlie) and Defiance Dolerite (St Ives).|Six sub-units: cumulate pyroxenite, melanocratic dolerite with pyroxene phenocrysts to 2cm, equigranular magnetite-rich dolerite, magnetite granophyre, fine-grained oxide-rich dolerite, fine-grained chilled zone.|
26841|Pernatty Dolerite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2696 Ma (inferred).|Leviathan Suite|||Differentiated sill: basal pyroxenite to dolerite; granophyric phase in the upper section; metamorphosed.|
26841|Pernatty Dolerite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2696 Ma (inferred)|Unit of Leviathan Suite.|||Differentiated sill: basal pyroxenite to dolerite; granophyric phase in the upper section; metamorphosed|
26841|Pernatty Dolerite|72095|5|Briefly described|p10-17, 21|||Kambalda Region, Eastern Goldfields, Yilgarn Craton. Compositionally indistinguishable from to High-Th Siliceous Basalt (HTSB) of Barnes et al., 2012. Detailed geochemistry is described.||||||
26841|Pernatty Dolerite|73391|6|Mentioned|Appendices.|||Langsford (1989). Regional stratigraphic correlation chart of other workers.|||||Differentiated dolerite, cumulate pyroxenite, gabbro.|
38554|Perseverance Ultramafic Complex|23862|4|Described|p31|Archean|Archean|Unit referred to as PUC.  Comparisons made with planetary volcanism.  Geological Province: Yilgarn Craton.||||||07-NOV-08
38554|Perseverance Ultramafic Complex|24395|3|Fully described|p201-202|Archean|Archean|In Harmony and Rocky's Rewards areas, has named horizons with it; Perseverance Ultramafic Horizon amd Rocky's Reward Horizon.||||||07-NOV-08
38554|Perseverance Ultramafic Complex|63712|5|Briefly described|p838|||Characterised by lens/pod accumulations of olivine accumulate - as in the Mount Keith and Six Mile Well Ultramafic Complexes.||||||15-JAN-08
38554|Perseverance Ultramafic Complex|70275|5|Briefly described|p482, 485-486, 488-489, 496, 499|||Leinster area, Agnew-Wiluna Belt, Yilgarn Craton. Located within the broader Perseverance ultramafic unit. A prominent lens associated with the Perseverance mine, where it is over 600mk thick (less than 25m thick in the Eleven Mile Well area). Interpreted as a giant lava pathway proximal to the vent.|||||Olivine adcumulate core (up to 94.5% fosterite) mantled by meso- to orthocumulate lithologies. Dunite flanked by serpentinite, pyroxenites and gabbros. Hosts Ni mineralisation.|
38554|Perseverance Ultramafic Complex|70863|6|Mentioned|p6, p12 Fig.9, p13|||Yilgarn Craton. 7 km long and 800m thick unit. Hosts the Perseverance deposit. Exploration involved detecting crustal contamination by assimilation of fractionated material into the magma. Appears as Perseverance ultramafic complex; abbreviated to PUC in places.|||||Komatiitic olivine meso- to adcumulates; sulphides at the basalt contact with a rhyodacite footwall. Has undergone polyphase deformation at amphibolite facies metamorphism.|
38554|Perseverance Ultramafic Complex|73596|6|Mentioned|p1156|Neoarchean|Neoarchean|Agnew-Wiluna Greenstone Belt. Presented as Perseverance Ultramafic Unit.|c.2715 Ma (maximum eruption age).|||Equivalent to Mount Keith Ultramafic Unit. Lateral equivalent to Agnew Komatiite.||
69789|Perth Formation|63745|2|Defined|p65-67, p73,  p78 Appx.|Late Pleistocene|Late Pleistocene|Parts previously mapped as Guildford Fm. Unconformable on Kings Park, Ascot, Yoganup and Guildford Fms; unconformable below Swan River Fm. Thick:13.5m. Interbedded alluvial sands, silts and clays + tripartite division of seds. See also p59, p62 Fig. 2b.||||||07-FEB-11
69789|Perth Formation|67135|6|Mentioned|p59 Fig.80.|||Shown as a unit suitable for clay mining.||||||
74953|Peter Well Granodiorite|64891|5|Briefly described|p37 Fig. 2, p41, p42, p48-9 Tb. 1|Archean|Archean|Of Eelya Suite (Annean Supersuite). Age: 2747+/-6Ma. Geological province: Murchison Domain. Subvolcanic intrusion into Greensleeves Formation, of biotite granodiorite; weakly metamorphosed.||||||07-FEB-11
74953|Peter Well Granodiorite|68698|5|Briefly described|p10|||Geochemistry described.||Eelya Suite.||||
74953|Peter Well Granodiorite|69583|5|Briefly described|p49|Neoarchean|Neoarchean|Murchison Domain.||Eelya Suite.||||
74953|Peter Well Granodiorite|69584|5|Briefly described|p5 Fig.2|Neoarchean|Neoarchean|||Eelya Suite|||Granodiorite.|
74953|Peter Well Granodiorite|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Eelya Suite.||||
74953|Peter Well Granodiorite|70030|5|Briefly described|p189-p190,205,207-208|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton. Synchronous with Polelle Group sedimentation, and possible driver of Hollandaire hydrothermal system. Dimensions: ~5-10 km in diameter and ~2km away from the Hollandaire massive sulfide. Similar geochemistry and age data to coherent rhyodacite associated with the Hollandaire deposit.|2759+\-2 Ma|Unit of Eelya Suite.||||17-JUL-19
74953|Peter Well Granodiorite|71168|5|Briefly described|p7, p22, p60|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. HFSE-enriched. Age also referenced in Van Kranendonk et al., 2013.|2747 +/- 6 Ma (U-Pb, Wang, 1998)|Eelya Suite||||
35234|Petermarer Monzogranite|24166|4|Described|p17|Archean|Archean|Of the Pippingarra Granitoid Complex.||||||07-NOV-08
35234|Petermarer Monzogranite|24327|5|Briefly described|Map Legend|Archean|Archean|Of the Pippingarra Granitoid Complex. Biotite-monzogranite.  Age: c.2940Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
35234|Petermarer Monzogranite|24349|5|Briefly described|Map legend|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
35234|Petermarer Monzogranite|50302|5|Briefly described|Map Legend|Archean|Archean|Part of Pippingarra Granitoid Complex.  Geological Province:  Pilbara Craton.  (See Bedrock chart).||||||07-NOV-08
35234|Petermarer Monzogranite|63420|5|Briefly described|Map legend|Archean|Archean|Of the Sisters Supersuite. Geological Province: Pilbara Craton. Biotite monzogranite; strongly  K-feldspar porphyritic to seriate; massive to weakly foliated; locally with strong flow alighnment; locally abundant inclusions; metamorphosed.||||||07-NOV-08
35234|Petermarer Monzogranite|63441|5|Briefly described|p11 Tb. 2|Archean|Archean|Of Sisters Supersuite. Geological province: Pilbara Craton.||||||07-FEB-11
35234|Petermarer Monzogranite|68281|6|Mentioned|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton. Age constrained by the parent Sisters Supersuite.||Of the Sisters Supersuite.||||23-SEP-13
35234|Petermarer Monzogranite|68283|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.||Of the Sisters Supersuite.||Includes locally abundant inclusions of Chillerina Granodiorite.|Biotite monzogranite; strongly K-feldspar porphyritic to seriate; massive to weakly foliated; locally with strong flow alignment; metamorphosed.|19-JUN-14
35234|Petermarer Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Sisters Supersuite|||Biotite monzogranite; seriate to strongly K-feldspar porphyritic; weakly metamorphosed|
35234|Petermarer Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; North Pilbara Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|2954-2919 Ma (inferred)|Unit of Sisters Supersuite.|||Biotite monzogranite; seriate to strongly K-feldspar porphyritic; weakly metamorphosed|
35234|Petermarer Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
35234|Petermarer Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||2940+/-2 Ma|Sisters Supersuite|||Biotite monzogranite; seriate to strongly K-feldspar porphyritic; weakly metamorphosed.|
33449|Petroglyph Gneiss|23416|5|Briefly described|Map Legend|Archean|Archean|Of Yule Granitoid Complex, Pilbara Craton||||||07-NOV-08
33449|Petroglyph Gneiss|23755|5|Briefly described|p54|Archean|Archean|Age: c.3470 Ma. See also page 18 Table 2. Geological Province: Yule Granitoid Complex.||||||07-NOV-08
33449|Petroglyph Gneiss|23813|5|Briefly described|p103|Archean|Archean|Age: 3470Ma.  Geological Province: Pilbara Craton.  See also p91 Tb. 1.||||||07-NOV-08
33449|Petroglyph Gneiss|24531|5|Briefly described|p8-9 Fig. 3|Archean|Archean|Of the Yule Granitoid Complex.||||||07-NOV-08
33449|Petroglyph Gneiss|24532|5|Briefly described|Map legend|Archean|Archean|Of Yule Granitoid Complex.  Tonalitic orthogneiss with sheets of white leucogranite.  Age: c.3420Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
33449|Petroglyph Gneiss|50379|5|Briefly described|Map Legend|Archean|Archean|Of Yule Granitoid Complex. Geological Province: Pilbara Craton. Age: c. 3470 Ma||||||07-NOV-08
33449|Petroglyph Gneiss|63441|5|Briefly described|p7 Tb. 2|Archean|Archean|Of the Tambina Supersuite. Age: c.3420Ma. Geological province: Pilbara Craton.||||||07-FEB-11
33449|Petroglyph Gneiss|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Tambina Supersuite. Age shown as c.3428 Ma. Tonalitic orthogneiss with sheeted pegmatitic granitic veins and local white leucogranite.||||||
33449|Petroglyph Gneiss|68282|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Tambina Supersuite||Includes sheets and patches of Kavir Granodiorite and Tambourah Monzogranite.|Tonalitic orthogneiss with sheeted pegmatitic granitic veins and local white leucogranite; with sheets of strongly foliated biotite granodiorite (Kavir Granodiorite) and patches of coarse-grained to pegmatite leucogranite (Tambourah Monzogranite).|
33449|Petroglyph Gneiss|69013|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane. An unnamed sub-unit, of foliated to gneissic granitic rock with abundant mafic and ultramafic xenoliths, is mapped separately.|c. 3428 Ma|Of the Tambina Supersuite.|||Comprises tonalitic orthogneiss with sheeted pegmatitic granite veins and local white leucogranite.|29-APR-14
33449|Petroglyph Gneiss|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c. 3428 Ma|Of the Tambina Supersuite.|||Tonalitic orthogneiss with sheeted pegmatitic granitic veins and local white leucogranite.|01-MAY-14
33449|Petroglyph Gneiss|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Tonalitic gneiss, strongly foliated biotite granodiorite, tonalitic orthogneiss with sheets of metagranodiorite. Age derived from sample of biotite diorite (169019.1.pdf)|3428 Ma +/- 6 Ma (SHRIMP)|Tambina Supersuite|||Tonalitic orthogneiss with sheeted pegmatitic granitic veins and local white leucogranite. Foliated to gneissic granitic rock with abundant mafic and ultramafic xenoliths.|
33449|Petroglyph Gneiss|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Locally occurs as enclaves with Tambourah Monzogranite. Sample GSWA 169019 (bt-hbl qrtz diorite enclave in Tambourah Monzogranite) yielded an interpreted igneous crystallisation age of 3428+\-6 Ma for the diorite (weighted mean 207Pb/206Pb). Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|3428-3420 Ma (isotopic, inferred)|Unit of Tambina Supersuite.|||Tonalitic orthogneiss with sheeted pegmatitic granitic veins and white leucogranite; foliated to gneissic metagranitic rock with abundant mafic and ultramafic xenoliths.|
33449|Petroglyph Gneiss|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||felsic gneiss|
33449|Petroglyph Gneiss|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||Max age 3428+/-6 Ma, min~3420 Ma.|Tambina Supersuite|||Tonalitic orthogneiss with sheeted pegmatitic granitic veins and local white leucogranite.|
33439|Petter Calc-silicate|22904|5|Briefly described|p59||Paleoproterozoic|Of Camel Hill Metamorphics. Maximum depositional age given as 1944+/-5 Ma.||||||07-NOV-08
33439|Petter Calc-silicate|23485|4|Described|p18|Paleoproterozoic|Paleoproterozoic|Of Camel Hills Metamorphics. Geological Province: Gascoyne Complex.||||||07-NOV-08
33439|Petter Calc-silicate|23486|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Camel Hills Metamorphics. Geological Province: Gascoyne Complex.||||||07-NOV-08
33439|Petter Calc-silicate|23487|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Camel Hills Metamorphics. Geological Province: Gascoyne Complex.||||||07-NOV-08
33439|Petter Calc-silicate|23525|5|Briefly described|p4|||||||||
33439|Petter Calc-silicate|23781|4|Described|p38|||Of Camel Hills Metamorphics. Geological Province: Yilgarn Craton.||||||25-JAN-08
33439|Petter Calc-silicate|24544|4|Described|p3|Paleoproterozoic|Paleoproterozoic|Of Camel Hills Metamorphics. Calc-silicate rock, para-amphibolite, and pelitic and psammitic schist. Intruded by Erong Granite.||||||07-NOV-08
33439|Petter Calc-silicate|50218|5|Briefly described|p241 Fig. 3, p249|Orosirian|Orosirian|Of the Camel Hills Metamorphics. Calc-silicate schist and gneiss, para-amphibolite and biotite-rich schist. Geological Province: Errabiddy Shear Zone.||||||07-FEB-11
33439|Petter Calc-silicate|63866|4|Described|p158|Paleoproterozoic|Paleoproterozoic|Outcrops extensively in the Erabiddy Shear Zone.|2700-2600 Ma (SHRIMP U-Pb)|Camel Hill Metamorphics|||Calc-silicate gneiss.|
33439|Petter Calc-silicate|65545|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Camel Hills Metamorphics, Gascoyne Province. c. 1985 Ma. Calc-Silic gneiss; coarse plag-qtz-diops-tremolite and diops-plag rocks, and fine qtz-plag-garnet hornblende rock.||||||
33439|Petter Calc-silicate|65896|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Camel Hills Metamorphics. Calc-silicate gneiss; coarse-grained plagioclase-quartz-diopside-tremolite and diopside-plagioclase rock, and fine-grained quartz-plagioclase-garnet-hornblende rock. Shown as equivalent age to Quartpot Pelite.||||||
33439|Petter Calc-silicate|66299|5|Briefly described|p4 Fig.2, p6 Fig.3, pp95-103.|Paleoproterozoic|Paleoproterozoic|Sourced from Yilgarn Craton.|Between 2608 and 1959 Ma.|Unit in Camel Hills Metamorphics.||Intruded by Moorarie Supersuite.|Calc-silicate schist or gneiss, commonly interlayered with amphibolite; minor quartzite.|
33439|Petter Calc-silicate|66887|5|Briefly described|p3 Fig.2, p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, southern Gascoyne Province.|~2600-~2000 Ma estimated from Fig.4.|Camel Hills Metamorphics||||
33439|Petter Calc-silicate|66950|5|Briefly described|p7, p9 Fig.8|Statherian|Neoarchean||c. 2610-1965 Ma|Of the Camel Hills Metamorphics.|||Comprises calc-silicate gneiss and schist with quartzite.|
33439|Petter Calc-silicate|67247|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, Gascoyne Province.|2001 - 1955 Ma.|Unit in Camel Hill Metamorphics.|||Calc-silicate gneiss; coarse-grained plagioclase-quartz-diopside-tremolite and diopside-plagioclase rocks, and fine-grained quartz-plagioclase-garnet-hornblende rock.|
33439|Petter Calc-silicate|67843|4|Described|p10, 23 and throughout the article.|Archean|Archean|Glenburgh Terrane. Deposition as part of the Yilgarn Craton passive margin. A raft occurs within Erong Granite, 2.5 km NNW of Erong homestead. Has entirely different detrital zircon population from Quartpot Pelite; sourced only from Archean rocks (Yilgarn Craton).|2608 +/- 4 Ma - max age of deposit of protolith.|Unit in Camel Hills Metamorphics.|||Calc-silicate schist and gneiss, interlayered with quartzite and quartz-diopside rock; minor pelitic schist or migmatitic pelitic gneiss and amphibolite.|20-NOV-13
33439|Petter Calc-silicate|69003|6|Mentioned|p10 Fig.10|||Fore-arc deposits to the Dalgaringa Arc.||||||
33439|Petter Calc-silicate|69080|6|Mentioned|p686 Fig.4|||Yilgarn Craton.||||||
33439|Petter Calc-silicate|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|||Camel Hills Metamorphics|||Calc-silicate gneiss; coarse-grained plagioclase--quartz--diopside--tremolite and diopside--plagioclase rocks, and fine-grained quartz--plagioclase--garnet--hornblende rock|
33439|Petter Calc-silicate|69387|5|Briefly described|p6, p23|||Coeval with Dalgaringa Supersuite. SG and magnetic susceptibility values given.||Camel Hills Metamorphics.||||
33439|Petter Calc-silicate|69583|6|Mentioned|p159 Fig.9|||Deposited between the converging Narryer Terrane (Yilgarn Craton) and Glenburgh Terrane (Gascoyne Province).||||||
33439|Petter Calc-silicate|69596|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|Yilgarn Craton. Appears as Petter calc-silicate.||||||
33439|Petter Calc-silicate|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_geologyl_lut.csv, 100k_interpgeop_lut.csv|2001-1955 Ma||||Calc-silicate gneiss; coarse-grained plagioclase-quartz-diopside-tremolite and diopside-plagioclase rocks, and fine-grained quartz-plagioclase-garnet-hornblende rock. Quartzite and quartz diopside rock.|
33439|Petter Calc-silicate|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||calc-silicate rock, para-amphibolite, pelite, psammite|
33439|Petter Calc-silicate|71269|4|Described|1m_geologyp12_lut.csv|||Geological province: Gascoyne Province, Glenburgh Terrane, Capricorn Orogen, West Australian Craton. Of Gascoyne Complex.||Unit of Camel Hills Metamorphics.|||Coarse calc-silicate gneiss, para-amphibolite, and pelitic and psammitic schist, minor quartzite and quartz diopside rock.|
72568|Phacopid Gully Bed|62735|5|Briefly described|p982|Frasnian|Frasnian|Informally named horizon within the Virgin Hills Formation. On the eastern side of the McWhae Ridge. Geological Province: Canning Basin.||||||
40078|Pierre Shale|24205|6|Mentioned|p242, p252|||Geological Province: Northern Carnarvon Basin.||||||
73392|Pig Well Formation|65147|6|Mentioned|p3, p4 Fig.3, p5 Fig.4, p7, p10-11    |Neoarchean|Neoarchean|Throughout this publication, this unit is called Pig Well-Yilgangi Formation, combining two formal names (Pig Well Formation and Yilgangi Conglomerate) into one informal name attributed to Groenewald and Goscombe, in press (as at 2006). Minimum age from intrusive stocks and dykes.|>2662 +/- 5 Ma (SHRIMP U-Pb zircon; Nelson, 1996)||||Lithic to feldspathic sandstone, coarse-grained, pebbly.|
73392|Pig Well Formation|65180|5|Briefly described|map legend|Archean|Archean|Metamorphosed polymictic conglomerate and sandstone of the Yilgarn Craton.||||||24-NOV-09
73392|Pig Well Formation|69152|4|Described|minerie_lut. files||Archean|Laverton Domain, Kurnalpi Terrane, Yilgarn Craton|||Includes 3 unnamed subunits.||Polymictic conglomerate, sandstone; lithic wacke; metamorphosed.|07-AUG-15
73392|Pig Well Formation|70153|5|Briefly described|Minerie_100k_geologyp_lut.csv|Archean|Archean|See also minerie_100k_interpgeop_lut. csv. Laverton Domain, Kurnalpi Terrane.|||||Polymictic conglomerate, sandstone, lithic wacke; metamorphosed.|
73392|Pig Well Formation|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, minerie_100k_geologyp_lut.csv.|2664+\-4 Ma; 2662+\-5 Ma||||Polymictic conglomerate and wacke; minor shale; metamorphosed|
73392|Pig Well Formation|72491|6|Mentioned|p5 Fig.4|||Kurnalpi Terrane, Yilgarn Craton.||||||
73392|Pig Well Formation|73596|6|Mentioned|p1161|Neoarchean|Neoarchean||2664 +/- 4 Ma (MDA).||||Coarse clastic rocks.|
34922|Pigeon Rocks Monzogranite|22902|5|Briefly described|68|||Geol province Southern Cross Province. Age 2729 +- Ma||||||
34922|Pigeon Rocks Monzogranite|23532|5|Briefly described|Map legend||Archean|Age:  c.2729 Ma. Yilgarn Craton||||||07-NOV-08
34922|Pigeon Rocks Monzogranite|23787|5|Briefly described|p14|Archean|Archean|Age: 2729+/-4Ma (SHRIMP U-Pb).  See also p50.  Geological Province: Yilgarn Craton.||||||07-NOV-08
34922|Pigeon Rocks Monzogranite|24167|6|Mentioned|p39|||||||||
34922|Pigeon Rocks Monzogranite|24245|5|Briefly described|p7 Tb. 1|Archean|Archean|Granitoid intrusion.  Age: c.2.73Ga.  Geological Province: Yilgarn Craton.||||||07-NOV-08
34922|Pigeon Rocks Monzogranite|24306|5|Briefly described|p943|Archean|Archean|Age: 2729 +/- 4Ma.   Geological Province: Yilgarn Craton||||||07-NOV-08
34922|Pigeon Rocks Monzogranite|63778|5|Briefly described|p1125 Fig. 1, p1126 Tb. 1, p1126, p1129|Archaean|Archaean|Age: 2729+/-4Ma (U-Pb zircon). Geological Province: Yilgarn Craton. More detailed information throughout the text.||||||18-MAR-09
34922|Pigeon Rocks Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Youanmi Terrane.|2729+/-4 Ma||||Biotite monzogranite; equigranular; metamorphosed.|
26102|Piker Hills Formation|22550|6|Mentioned|Fig 3|||||||||
26102|Piker Hills Formation|22741|5|Briefly described|P21, P24, Table3 P16||Devonian|||||||
26102|Piker Hills Formation|22776|6|Mentioned|p17|||Equivalent to Clanmeyer Siltstone.||||||10-NOV-08
26102|Piker Hills Formation|23338|5|Briefly described|915 Fig.3|Famennian|Famennian|||||||
26102|Piker Hills Formation|23847|5|Briefly described|p297|Famennian|Famennian|Geological Province: Canning Basin.||||||
26102|Piker Hills Formation|23903|5|Briefly described|p1597 Fig.2|Famennian|Famennian|Geological Province: Canning Basin.||||||10-NOV-08
26102|Piker Hills Formation|24061|5|Briefly described|p180|||Geological Province: Canning Basin.||||||28-MAY-08
26102|Piker Hills Formation|24503|5|Briefly described|Map legend|Devonian|Devonian|Geological Province: Canning Basin.||||||
26102|Piker Hills Formation|31152|6|Mentioned|Fig. 3|||||||||
26102|Piker Hills Formation|31332|6|Mentioned|Fig. 3|||||||||
26102|Piker Hills Formation|32594|4|Described|p3|||Refers fossil content||||||
26102|Piker Hills Formation|32647|6|Mentioned|p98|||||||||
26102|Piker Hills Formation|32865|6|Mentioned|p474|||Fauna||||||
26102|Piker Hills Formation|33042|6|Mentioned|p725|||See also Fig.2. Dev.||||||
26102|Piker Hills Formation|34427|6|Mentioned|Fig.3|||||||||
26102|Piker Hills Formation|35104|6|Mentioned|p5|||||||||
26102|Piker Hills Formation|36225|6|Mentioned|Map legend|Famennian|Famennian|||||||
26102|Piker Hills Formation|36365|6|Mentioned|p820|||||||||
26102|Piker Hills Formation|36890|3|Fully described|p333|||||||||
26102|Piker Hills Formation|39702|6|Mentioned|Fig.2|||||||||
26102|Piker Hills Formation|40793|6|Mentioned|Fig.3|||||||||
26102|Piker Hills Formation|40797|6|Mentioned|Fig.2|||||||||
26102|Piker Hills Formation|41111|6|Mentioned|Fig.4|||||||||
26102|Piker Hills Formation|41139|6|Mentioned|Fig.2|||||||||
26102|Piker Hills Formation|41894|6|Mentioned|p5|||||||||
26102|Piker Hills Formation|42030|6|Mentioned|p748|||||||||
26102|Piker Hills Formation|42080|6|Mentioned|p281|||||||||
26102|Piker Hills Formation|42111|6|Mentioned|Text fig.3 P90|||||||||
26102|Piker Hills Formation|42347|6|Mentioned|Fig.2 P1020|||||||||
26102|Piker Hills Formation|42351|5|Briefly described|Fig.3 P40|||||||||
26102|Piker Hills Formation|42564|5|Briefly described|Fig.5, 6 P6|||||||||
26102|Piker Hills Formation|42880|5|Briefly described|Fig.2,p1020|||||||||
26102|Piker Hills Formation|43173|6|Mentioned|54||Late Devonian|||||||
26102|Piker Hills Formation|43563|6|Mentioned|Fig.5,p10||Late Devonian|||||||
26102|Piker Hills Formation|44143|4|Described|p437 Table 4-19, p442, p443 Fig. 4-98|Devonian|Devonian|Up to 300m thick; calcarenite, calcirudite, shale and siltstone; shallow marine. Interfingers with Windjana Limestone. Type section at Piker Hills (MOUNT RAMSAY: 18deg 04' 30" S, 126 deg 05' 30" E). Contains ammonoids, conodonts and brachiopods; late Famennian. Appears as Piker Hill Formation in Fig.4-98.||||||24-NOV-17
26102|Piker Hills Formation|44231|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Fore-reef subfacies and basin facies; calcarenite, limestone breccia and megabreccia, sandstone, siltstone, and minor conglomerate. Geological Province: Canning Basin.||||||26-MAY-05
26102|Piker Hills Formation|44397|14|Not recorded|p.12, Figs.2,3,Tb.4||Famennian|||||||
26102|Piker Hills Formation|44398|14|Not recorded|map legend||Famennian|||||||
26102|Piker Hills Formation|45041|6|Mentioned|Fig.45|||Famennian||||||
26102|Piker Hills Formation|45063|6|Mentioned|Fig. 9|||Dev.||||||
26102|Piker Hills Formation|45101|5|Briefly described|p7|||See also P22. Conodont content||||||
26102|Piker Hills Formation|45133|6|Mentioned|p4|||||||||
26102|Piker Hills Formation|45143|3|Fully described|Fig.3|||Time-stratigraphic interpretations.||||||
26102|Piker Hills Formation|45153|2|Defined|App.3-49|Famennian|Famennian|||||||
26102|Piker Hills Formation|45158|4|Described|p24|||||||||
26102|Piker Hills Formation|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
26102|Piker Hills Formation|63938|5|Briefly described|p50 Fig.2|Famennian|Famennian|||||||
26102|Piker Hills Formation|64159|5|Briefly described|p91 Fig. 6|Famennian|Famennian|Part of the Lennard Reef facies development. Mainly a siltstone unit.||||||
26102|Piker Hills Formation|64502|5|Briefly described|p764, p765 Fig. 2|Famennian|Famennian|||||||
26102|Piker Hills Formation|64580|5|Briefly described|map legend|||Famennian reef complexes, marginal slope and basin facies.||||||10-NOV-08
26102|Piker Hills Formation|64643|5|Briefly described|p7 Fig. 5, p35|||Marginal slope facies.||||||24-NOV-08
26102|Piker Hills Formation|65214|6|Mentioned|p280|Devonian|Devonian|Canning Basin. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
26102|Piker Hills Formation|65486|5|Briefly described|p6 Fig.5, Plate 1.|Late Famennian|Middle Famennian|Marginal-slope and basin limestone, sandstone and siltstone, Canning Basin. Overlies Virgin Hills Formation. Unconformably underlies Fairfield Group.||||||
26102|Piker Hills Formation|66127|3|Fully described|pp19-21, pp61-62, p80, Plates 3,7,8|Famennian|Famennian|Of Playford and Lowry (1966), after Piker Hills, the type locality on Fossil Downs Station. Poorly exposed. Fossils dominated by brachiopods.||||Conformably overlies Virgin Hills Formation; interfingers with and abuts Windjana and Nullara Limestones, and interfingers with Barramundi and Stony Creek Conglomerates. Underlies Fairfield Group.|Basin facies: interbedded shale, siltstone, and limestones grading into sandstone or conglomerate. Marginal-slope facies: limestone, locally dolomitized; allochthonous limestone blocks and debris-flows.|
26102|Piker Hills Formation|67131|6|Mentioned|p3 Fig. 2,|Famennian|Famennian|Marginal-slope and basin facies.||||Overlies Virgin Hills Formation. Overlain by Gumhole Formation.||
26102|Piker Hills Formation|68298|5|Briefly described|p234|Famennian|Famennian|An anterior median dorsal plate of Remigolepis is recorded (J. Long, pers. comm.).||||||24-JAN-13
26102|Piker Hills Formation|69099|5|Briefly described|500k_geologyp08_lut.csv|Fammenian|Fammenian|Famennian reef complexes, marginal slope and basin facies. Grouped as Piker Hills Formation, Bugle Gap Limestone, upper Napier Formation and upper Virgin Hills Formation in 500k_geologyp08_lut.csv.||||||
26102|Piker Hills Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Famennian|Famennian|||||||
26102|Piker Hills Formation|70492|6|Mentioned|p179|||SE Lennard Shelf, Canning Basin.||||||
26102|Piker Hills Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Fossiliferous shallow marine reef to marginal slope and basin facies calcarenite, calcirudite, calcilutite, with minor interbedded shale and siltstone|
26102|Piker Hills Formation|71811|5|Briefly described|Map legend.|Famennian|Famennian|Canning Basin. A unit in the Devonian Reef Complexes: Famennian marginal slope and basin facies.|||||Yellow and grey limestone, siltstone and sandstone, locally conglomeratic (in debris flows).|06-MAY-19
26102|Piker Hills Formation|72502|6|Mentioned|p5|Famennian|Famennian|Lennard Shelf, Canning Basin.||||Underlain by Virgin Hills Formation. Equivalent to Napier Formation and Bugle Gap Formation.||
35352|Pilbara Creek Monzogranite|50370|5|Briefly described|Map Legend|Archean|Archean|Of Yule Granitoid Complex. Geological Province: Pilbara Craton.||||||07-NOV-08
35352|Pilbara Creek Monzogranite|63372|4|Described|Map Legend|Archean|Archean|Of the Yule Granitoid Complex. Geological Province: East Pilbara Granite-Greenstone Terrane. Biotite-bearing monzogranite and syenogranite; leucocratic; weakly foliated to massive; metamorphosed.||||||07-NOV-08
35352|Pilbara Creek Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, syenogranite|
35352|Pilbara Creek Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Sisters Supersuite|||Biotite monzogranite and syenogranite; leucocratic; weakly foliated to massive; metamorphosed.|
42195|Pilga Leucogranite|50423|3|Fully described|p217, 219||Archean|Here differentiated as younger pluton distinct from North Shaw Suite. Quartz, plagioclase, K-feldspar, <5% biotite. Age difficult to determine due to inherited, igneous and metamorphic zircons; 3345-3300, probably 3345-3410 Ma. Of Shaw Granitoid Complex.||||||07-NOV-08
42195|Pilga Leucogranite|50427|4|Described|p186|Archean|Archean|Age: 3445-3410 Ma. Derived from partial melting of older tonalite-trondhjemite-granodiorite protoliths. Of Shaw Granitoid Complex.||||||07-NOV-08
42195|Pilga Leucogranite|63441|2|Defined|p7 Tb. 2, p35|Archean|Archean|Formerly included in North Shaw Suite but recent mapping + SHRIMP indicate it is not related. Of Tambina Supersuite. Age: c.3445+/-3Ma. Geol.prov: Pilbara Craton. Derived from the melting of sodic granitic protoliths in the core of Shaw Granitic Complex.||||||07-FEB-11
25744|Pillara Limestone|22550|6|Mentioned|Fig 3|||||||||
25744|Pillara Limestone|22741|5|Briefly described|P21, P23, Table3 P17||Early Devonian|||||||
25744|Pillara Limestone|22767|6|Mentioned|P11|||||||||
25744|Pillara Limestone|23185|6|Mentioned|p168|||||||||
25744|Pillara Limestone|23338|5|Briefly described|919|Famennian|Givetian|||||||
25744|Pillara Limestone|23522|5|Briefly described|p245|||||||||
25744|Pillara Limestone|23903|5|Briefly described|p1597 Fig.2|Famennian|Givetian|Geological Province: Canning Basin.||||||13-NOV-07
25744|Pillara Limestone|23979|5|Briefly described|p210|Frasnian|Givetian|Geological Province: Canning Basin.||||||19-MAY-04
25744|Pillara Limestone|24061|5|Briefly described|p180|Late Devonian|Middle Devonian|Of "Lennard River Group".  Geological Province:  Canning Basin.||||||
25744|Pillara Limestone|24062|5|Briefly described|p186 Table 1|Devonian|Devonian|Geological Province: Canning Basin.||||||
25744|Pillara Limestone|24390|5|Briefly described|p8|Devonian|Devonian|Geological Province: Canning Basin.||||||
25744|Pillara Limestone|30110|6|Mentioned|p81|||See also p82. Upper Devonian, Frasnian - Famennian age.||||||25-FEB-08
25744|Pillara Limestone|30181|6|Mentioned|p178|||||||||
25744|Pillara Limestone|30187|6|Mentioned|p179|||||||||
25744|Pillara Limestone|30525|6|Mentioned|Map legend|Famennian|Frasnian|Famennian to Frasnian.||||||25-FEB-08
25744|Pillara Limestone|30526|6|Mentioned|p118|||Devonian age.||||||25-FEB-08
25744|Pillara Limestone|30533|4|Described|p24|||On Table 6.||||||13-NOV-07
25744|Pillara Limestone|30896|4|Described|p19|||||||||
25744|Pillara Limestone|30897|4|Described|p18|||||||||
25744|Pillara Limestone|30898|6|Mentioned|Map legend|Famennian|Frasnian|Frasnian - Famennian.||||||25-FEB-08
25744|Pillara Limestone|31151|6|Mentioned|p68|||||||||
25744|Pillara Limestone|31152|6|Mentioned|p2|||||||||
25744|Pillara Limestone|31226|6|Mentioned|Map legend|Famennian|Frasnian|Frasnian - Famennian.||||||25-FEB-08
25744|Pillara Limestone|31332|6|Mentioned|Fig. 3|||||||||
25744|Pillara Limestone|32594|6|Mentioned|p3|||Refers Playford and Lowry (1966).||||||25-FEB-08
25744|Pillara Limestone|32619|6|Mentioned|p464|||Givetian.||||||25-FEB-08
25744|Pillara Limestone|32647|1|Redefined|p100|Frasnian|Frasnian|Name superseded by Pillara Formation RDEF 87/25751.||||||
25744|Pillara Limestone|32648|6|Mentioned|p32|||Dev.||||||
25744|Pillara Limestone|32865|6|Mentioned|p471|||See also p472. Givetain to Frasnian and Famennian.||||||25-FEB-08
25744|Pillara Limestone|33042|6|Mentioned|p723|||Frasnian. See also pp725, 731-734, 745 etc.||||||25-FEB-08
25744|Pillara Limestone|33621|6|Mentioned|p183|||||||||
25744|Pillara Limestone|34427|6|Mentioned|Fig.3|||||||||
25744|Pillara Limestone|34484|6|Mentioned|p22|||||||||
25744|Pillara Limestone|34999|6|Mentioned|p124|||||||||
25744|Pillara Limestone|35104|6|Mentioned|p5|||||||||
25744|Pillara Limestone|35275|6|Mentioned|Fig.5.|||||||||
25744|Pillara Limestone|35980|6|Mentioned|p131|||||||||
25744|Pillara Limestone|36225|6|Mentioned|Map legend|Frasnian|Givetian|Givetian to Frasnian.||||||25-FEB-08
25744|Pillara Limestone|36257|6|Mentioned|Table 2.1|||||||||
25744|Pillara Limestone|36365|6|Mentioned|p815|||||||||
25744|Pillara Limestone|36890|3|Fully described|p331|||Formerly Pillara Formation.||||||13-NOV-07
25744|Pillara Limestone|38207|6|Mentioned|Fig.1|||||||||
25744|Pillara Limestone|39702|6|Mentioned|Fig.2|||||||||
25744|Pillara Limestone|40236|6|Mentioned|Fig.5|||||||||
25744|Pillara Limestone|40793|6|Mentioned|p164|||||||||
25744|Pillara Limestone|40797|6|Mentioned|p155|||||||||
25744|Pillara Limestone|40866|6|Mentioned|p179|||||||||
25744|Pillara Limestone|41139|6|Mentioned|Fig.2|||||||||
25744|Pillara Limestone|41158|6|Mentioned|p80|||||||||
25744|Pillara Limestone|41215|6|Mentioned|p275|||||||||
25744|Pillara Limestone|41512|6|Mentioned|p30|||||||||
25744|Pillara Limestone|41894|4|Described|p3|||||||||
25744|Pillara Limestone|41918|5|Briefly described|p103|||||||||
25744|Pillara Limestone|42030|5|Briefly described|p747|||||||||
25744|Pillara Limestone|42073|6|Mentioned|Fig.2 P292|||||||||
25744|Pillara Limestone|42080|6|Mentioned|p281|||||||||
25744|Pillara Limestone|42111|5|Briefly described|p88|||See also Text fig.3||||||
25744|Pillara Limestone|42176|6|Mentioned|p204|||See also Fig.2.||||||25-FEB-08
25744|Pillara Limestone|42347|5|Briefly described|Fig.4 P1021, Fig.2|||See also Fig.9 p1026.||||||13-NOV-07
25744|Pillara Limestone|42351|5|Briefly described|p40|||See also Fig.3 p40, Fig. 4 p41.||||||13-NOV-07
25744|Pillara Limestone|42473|6|Mentioned|p7|||||||||
25744|Pillara Limestone|42564|5|Briefly described|p9|||||||||
25744|Pillara Limestone|42710|5|Briefly described|map legend|Late Devonian||||||||
25744|Pillara Limestone|42811|4|Described|p40|||see also Fig.9.||||||13-NOV-07
25744|Pillara Limestone|42860|5|Briefly described|Fig.2|||||||||
25744|Pillara Limestone|42880|5|Briefly described|Fig.2,p1020|||||||||
25744|Pillara Limestone|42930|5|Briefly described|Fig.1 p473|Late Devonian|Devonian|Interfingers with Sadler Limestone. Partly overlies Mellinjerie Limestone. Geological Province: Canning Basin.||||||13-NOV-07
25744|Pillara Limestone|42933|5|Briefly described|Fig.94 p258|||||||||
25744|Pillara Limestone|42977|5|Briefly described|p274|||||||||
25744|Pillara Limestone|43173|5|Briefly described|12, 54||Late Devonian|||||||
25744|Pillara Limestone|43281|6|Mentioned|Map legend||Late Devonian|||||||
25744|Pillara Limestone|43581|5|Briefly described|p39|||||||||
25744|Pillara Limestone|43666|6|Mentioned|p7||Late Devonian|||||||
25744|Pillara Limestone|43723|6|Mentioned|p51||Devonian|||||||
25744|Pillara Limestone|43818|6|Mentioned|p38|||||||||
25744|Pillara Limestone|43819|6|Mentioned|p31||Late Devonian|||||||
25744|Pillara Limestone|43823|6|Mentioned|p755,Fig.2,|||||||||
25744|Pillara Limestone|44143|4|Described|p438 Table 4-19, p442, p443 Figure 4-98|Devonian|Devonian|Up to 450m thick; limestone and minor dolomite; shallow marine. Interfingers with Napier Formation and Sadler Limestone. Type section at Menyous Gap in the Pillara Range (NOONKANBAH: 18deg 24' S, 125deg 56' E). Contains brachiopods, atrypids, bivalves, corals and bryozoans; Givetian to Frasnian.||||||24-NOV-17
25744|Pillara Limestone|44231|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Platform facies - back reef, reef flat and reef margins subfacies; biostromal back-reef stromatoporoid, coral, and cyanobacterial limestone; cyclic interbeds of sst, sltst., and minor conglomerate; rimmed by stromatopor. and cyanobact.reef framestones.||||||27-JAN-10
25744|Pillara Limestone|44366|14|Not recorded|p.19, Table 3|||Givetian (?) to Famennian.||||||
25744|Pillara Limestone|44367|14|Not recorded|map legend|||(Reprinted 1971), Givetian? to Famennian.||||||
25744|Pillara Limestone|44397|14|Not recorded|p.11,Figs.2,3,Tb.4|||Famennian to Givetian (?). See also p.12,18.||||||
25744|Pillara Limestone|44398|14|Not recorded|map legend|||Givetian (?) to Famennian.||||||
25744|Pillara Limestone|44993|14|Not recorded|p.22|||||||||
25744|Pillara Limestone|45015|5|Briefly described|p47|Frasnian|Frasnian|Name used interchangeably with Pillara Formation. Geological Province: Fitzroy Basin.||||||29-JAN-08
25744|Pillara Limestone|45039|6|Mentioned|Fig.5|||||||||
25744|Pillara Limestone|45063|6|Mentioned|p28|||See also Fig. 9 Dev.||||||
25744|Pillara Limestone|45101|6|Mentioned|p5|||See also p15, p21. Conodont content.||||||25-FEB-08
25744|Pillara Limestone|45133|6|Mentioned|Fig.6|||||||||
25744|Pillara Limestone|45143|3|Fully described|Fig.3|||Time-stratigraphic interpretations.||||||
25744|Pillara Limestone|45158|4|Described|p24|||||||||
25744|Pillara Limestone|46869|6|Mentioned|Fig.1|||||||||
25744|Pillara Limestone|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
25744|Pillara Limestone|48831|14|Not recorded|p.44-50,64|||||||||
25744|Pillara Limestone|48848|14|Not recorded|p.58|||||||||
25744|Pillara Limestone|48931|5|Briefly described|p61|||||||||
25744|Pillara Limestone|50085|5|Briefly described|p8|Devonian|Devonian|?Of the Gogo Formation.  Geological Province: Canning Basin.||||||13-NOV-07
25744|Pillara Limestone|60333|5|Briefly described|p802|Devonian|Devonian|Platform facies.||||||
25744|Pillara Limestone|62575|5|Briefly described|p665|Late Devonian|Late Devonian|Reef-margin subfacies - unbedded microbial-stromatoporoid reef limestone. Geological Province: Canning Basin. Text refers to "the Frasnian Pillara Sequence".||||||20-JUL-06
25744|Pillara Limestone|63110|6|Mentioned|p1135|||Age: 400Ma - 326Ma.||||||11-JUN-08
25744|Pillara Limestone|63938|4|Described|p48, 49, 51|Frasnian|Givetian|Platform facies. Reef margin and reef-flat. Overlies Cadjebut Formation where that unit occurs.||||||
25744|Pillara Limestone|64159|5|Briefly described|p91 Fig. 6|Famennian|Givetian|Part of the Lennard Reef facies development. Mainly a siltstone unit.||||||
25744|Pillara Limestone|64187|5|Briefly described|p320 Fig. 2|Frasnian|Frasnian|Underlain unconformably by Poulton Formation, overlain by Napier Formation. Limestone, sandstone (shallow marine). Geological Province: Canning Basin.||||||01-MAY-13
25744|Pillara Limestone|64502|4|Described|p765 Fig. 2, p766 Fig.3, p769|Frasnian|Givetian|Shows Early Permian glacial pavement features in Goongewa Mine. See p769.||||||27-JAN-10
25744|Pillara Limestone|64580|6|Mentioned|map legend|||Givetian-Frasnian reef complexes, platform facies.||||||15-DEC-08
25744|Pillara Limestone|64643|4|Described|p5 Fig. 4, p6, p7 Fig.5, 33-36|Frasnian|Givetian|Platform facies. Reef margin and reef-flat.||||||17-NOV-08
25744|Pillara Limestone|64783|6|Mentioned|p101|||Canning Basin.||||||15-NOV-17
25744|Pillara Limestone|64981|6|Mentioned|p670, p677.|Frasnian|Givetian|Lennard Shelf, Canning Basin. Reefal carbonates growing on pre-existing structural highs.||||||
25744|Pillara Limestone|65301|6|Mentioned|p8 Fig. 5|||||||||
25744|Pillara Limestone|65449|6|Mentioned|p47|||Overlies Carribuddy Group and/or Worral Formation in East Crab Creek 1. Appears only as Pillara.||||||
25744|Pillara Limestone|65486|5|Briefly described|p6-70, Plate 1.|Frasnian|Givetian|Reef complex, Canning Basin. Type section described. Unconformably underlies Nullara Limestone. Conformably underlies Sadler Limestone, Gogo Formation, Napier Formation. Unconformably overlies Prices Creek Group, Cadjebut Formation. Brittle microbial and stromatoporoid reef limestone. Karstified.||||||06-JAN-17
25744|Pillara Limestone|66127|3|Fully described|pp19-21, p26-42, p150-165, Plates 2 to 8|Late Frasnian|Late Givetian|Of Playford and Lowry (1966); formerly Pillara Formation of Guppy et al. (1958); name changed to reflect the dominant and most characteristic lithology. Named after Pillara Range; type section at Menyous Gap. Playford and Lowry used the name for all Givetian, Frasnian and Famennian back-reef carbonates on the Lennard Shelf; Playford (1980) limited it to Givetian and Frasnian platform deposits and allocated the Famennian material to Nullara (back-reef and bank) and Windjana (reef-margin and reef-flat) Limestones. Average thickness 1000 m. Richly fossiliferous, esp. stromatoporoids. Measured sections of sediment cyclicity discussed in great detail.||||Conformably overlies Cadjebut Formation and unconformably underlies Nullara and Windjana Limestones.|Three different reef facies are mapped separately. Platform facies: stromatoporoid, coralline and fenestral limestone grading into sandstone. Reef-margin facies: similar thick-bedded limestone. Fore-reef: large allochthonous Pillara Limestone blocks.|24-APR-17
25744|Pillara Limestone|67131|6|Mentioned|p3 Fig. 2,|Frasnian|Givetian|Reef, back-reef, and bank subfacies. Equivalent to Pillara Sequences 1-6.||||Overlain unconformably by Windjana Limestone, Nullara Limestone.|Limestone.|29-JAN-20
25744|Pillara Limestone|69099|5|Briefly described|500k_geologyp08_lut.csv|Frasnian|Givetian|Givetian-Frasnian reef complexes, platform facies||||Overlies Cadjebut Formation.||
25744|Pillara Limestone|69165|6|Mentioned|500k_geologyp08_lut.csv|Frasnian|Givetian|||||||
25744|Pillara Limestone|69182|6|Mentioned|Ch4 p30-p35, Ch4 p39|||Canning Basin. Excellent reservoir potential for the storage of carbon dioxide. See also Ch4 p44, Ch4 p65, Ch4 p78.||||||
25744|Pillara Limestone|69312|6|Mentioned|p19|Devonian|Devonian|Canning Basin. ||||Overlain by the Nullara Formation. Overlies the Virgin Hills Formation.|Limestone.|
25744|Pillara Limestone|70065|5|Briefly described|Rowley: Fig.2. Regional: Fig.4|Frasnian|Frasnian|Offshore Canning Basin.||Reef Complex.||Is overlain by Laurel Formation (Fairfield Group).||
25744|Pillara Limestone|70126|5|Briefly described|Map legend|Frasnian|Frasnian|Canning Basin. Devonian Reef Complex.|||||Massive to well-bedded, stromatoporoid and microbial limestone; locally dolomitized, locally sandy and grading to sandstone, commonly dolomitized; platform (generally back-reef) facies in carbonate reef complexes.|
25744|Pillara Limestone|70154|4|Described|100k_geologyp_lut.csv|Frasnian|Givetian||372-388 Ma||||Massive to well-bedded, stromatoporoid and microbial limestone; locally dolomitized, locally sandy and grading to sandstone, commonly dolomitized; platform (generally back-reef) facies in carbonate reef complexes.|
25744|Pillara Limestone|70272|5|Briefly described|p877, 882|Devonian|Devonian|Lennard shelf, Canning Basin. Hosts the Blendevale Zn-Pb deposit; Rb-Sr dating gives mineralisation ages around 357 +/- 3 Ma. Forms of mineralisation described.||||Is overlain by Fairfield Group.||
25744|Pillara Limestone|71146|6|Mentioned|p31 fig 25|Upper Devonian|Devonian|Northern Canning Basin. Deposited as reef-rflat and back reef subfacies.||||||
25744|Pillara Limestone|71267|4|Described|GEOL_LUT_CSV files|Frasnian|Givetian|Of Lennard Shelf, Canning Basin. Givetian-Frasnian reef complexes, platform facies. Events: Meda Transpression (323-310 Ma); Red Bluffs Extension (372.2-360 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma); Pillara Movement (Alice Springs Orogeny phase 2) (390-360 Ma); Van Emmerick Extension (382.7-372.2 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 100k_geologyp_lut.csv.|387.7-372.2 Ma (biostrat)||||Massive to well-bedded, stromatoporoid and microbial limestone; locally dolomitized, locally sandy and grading to sandstone, commonly dolomitized; platform (generally back-reef) facies in carbonate reef complexes|
25744|Pillara Limestone|71811|5|Briefly described|Map legend.|Frasnian|Givetian|Canning Basin. A unit in the Devonian Reef Complexes; platform facies (generally back-reef) in carbonate reef complexes.|||||Massive to well-bedded, stromatoporoid and microbial limestone; locally dolomitized, locally sandy and grading to sandstone.|06-MAY-19
25744|Pillara Limestone|71892|6|Mentioned|p10|Paleozoic|Paleozoic|||||||
25744|Pillara Limestone|72489|6|Mentioned|p12 Fig.9, p13 Fig.10|Devonian|Devonian|||||||
25744|Pillara Limestone|72502|6|Mentioned|p5|Frasnian|Givetian|Lennard Shelf, Canning Basin.||||Underlain by Cadjebut Formation. Overlain by Windjana Limestone and Nullara Limestone. Equivalent to Virgin Hills Formation and Sadler Limestone.||
30667|Pillara Monzogranite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1860Ma. Geological province: Kimberley Province (West).||||||07-FEB-11
30667|Pillara Monzogranite|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|Approx 1865 - 1850 Ma.||||||
30667|Pillara Monzogranite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite.||||||07-NOV-08
30667|Pillara Monzogranite|72437|5|Briefly described|p77|||Hooper Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Syenogranite and granodiorite.|
77577|Pillara Sequence|65486|5|Briefly described|p4|Frasnian|Givetian|Second-order Sequence. Is overlain unconformably by Nullara Sequence.||||||
77577|Pillara Sequence|66127|4|Described|p21 Fig.21, pp65-81.|Frasnian|Middle Givetian|Second-order sedimentary sequence. Includes basal Cadjebut Formation, Pillara and Sadler Limestones, Gogo and lower part of Virgin Hills Formations, Sparke and Elma Conglomerates. Six third-order sequences are described. Terminated by Frasnian-Famennian boundary event. About 1000 m thick; deposited over c.13 m.y.||||Is overlain by Nullara Sequence.||
77577|Pillara Sequence|69312|6|Mentioned|p3, p23 fig 27, p24 fig 28|Famennian|Givetian|Canning Basin. |||Includes the Gogo Formation ?|Overlies the Tandalgoo Sandstone. Overlain by the Nullara Sequence.|Carbonates.|11-FEB-20
77577|Pillara Sequence|70065|5|Briefly described|Regional: p6|Devonian|Devonian|Basal marine shales have fair to good petroleum generative potential, and are inferred to be present throughout the Oobagooma Sub-basin. Part of Larapintine 3 petroleum system.||||||01-MAY-19
31962|Pimbyana Granite|22660|4|Described|p 300|||local term p300.  This Unit intrudes quartzo-feldspathic migmatites.  Province - Edmund Batholith.||||||
31962|Pimbyana Granite|23774|5|Briefly described|p732 Fig 1||Paleoproterozoic|Age: 1829+/-13 Ma, 1791+/-10 Ma. Also see p743.  Of Gascoyne Complex.||||||07-NOV-08
31962|Pimbyana Granite|24197|6|Mentioned|p71 Tb. 7.1|||Of the Chararoo Supersuite.||||||07-FEB-11
31962|Pimbyana Granite|24544|5|Briefly described|p42|Statherian|Statherian|Age: 1670 Ma.||||||
31962|Pimbyana Granite|50216|5|Briefly described|p213|Paleoproterozoic|Paleoproterozoic|Of the northern Gascoyne Copmlex. Age: 1673+/-15 Ma (Nelson, 2002).||||||07-NOV-08
31962|Pimbyana Granite|50225|5|Briefly described|p388, p397|Paleoproterozoic|Paleoproterozoic|Age: c.1675Ma; c.1673Ma (Nelson, 2002).||||||07-FEB-11
31962|Pimbyana Granite|50292|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Complex. Age: 1675Ma.||||||07-NOV-08
31962|Pimbyana Granite|50425|5|Briefly described|p1.3, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Province. Of the Chararoo Supersuite. Age: 1674-1829 +/- 13Ma (U-Pb, Shrimp).||||||07-NOV-08
31962|Pimbyana Granite|61262|2|Defined|p459 App., p447 Fig. 4.|Paleoproterozoic|Paleoproterozoic|Of Durlacher Supersuite. Mostly biotite (-muscovite) monzogranite to syenogranite. Intrudes Gooche Gneiss and Pooranoo Metamorphics. Intruded by Dingo Creek and Yangibana Granites. Age: 1773+/-15Ma, 1673+/-11Ma and 1674+/-8Ma. Type locality included.||||||07-NOV-08
31962|Pimbyana Granite|63470|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Durlacher Supersuite. Geological Province: Gascoyne Complex. Massive, medium-grained, megacrystic and porphyritic biotite (-muscovite) monzogranite; tabular megacrysts of K-feldspar up to 7cm long.||||||07-NOV-08
31962|Pimbyana Granite|63866|5|Briefly described|p155, p160, p162|Statherian|Statherian|Emplaced during the Mangaroon Orogeny. Numeric age is SHRIMP U-Pb zircon age.|1673 +/- 15 Ma (Nelson, 2002)|Durlacher Supersuite||Intrudes the Pooranoo Metamorphics.||
31962|Pimbyana Granite|63869|4|Described|p12, p18, p19, p21, p22, p23, p24, p26|Paleoproterozoic|Paleoproterozoic|See also p29, Plate 1. Pearson et al., (1996); Martin et al., (2002). In EDMUND sheet, includes several large rafts of Gooche Gneiss. SHRIMP U-Pb zircon igneous crystallisation ages of syenogranite and monzogranite facies respectively. A biotite tonalite sample has an age of 1674 +/- 8 Ma.|1673 +/- 15 Ma; 1675 +/- 11 Ma (GSWA, 2005).|Unit in Durlacher Supersuite.||Intrudes Pooranoo Metamorphics. Is intruded by Dingo Creek and Yangibana Granites.|Most abundant rock is a coarse-grained porphyritic to megacrystic biotite(-muscovite) monzogranite to syenogranite; fine- to medium-grained biotite tonalite and granodiorite are abundant E and SE of Star of Mangaroon mine.|
31962|Pimbyana Granite|65830|6|Mentioned|p30-31, Plate 2|Statherian|Statherian|Contains 30-45% tabular K-feldspar phenocrysts 1.5-2cm long, commonly with a weak preferred orientation.|1675 +/- 11 Ma (GSWA, 2006).|Unit in Durlacher Supersuite.||Intruded by Dingo Creek Granite.|Coarse-grained strongly porphyritic biotite monzogranite.|
31962|Pimbyana Granite|66110|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Durlacher Supersuite. Massive, medium-grained, megacrystic and porphyritic biotite(-muscovite) monzogranite; tabular megacrysts of K-feldspar up to 7cm long.||||||
31962|Pimbyana Granite|66299|4|Described|p178, p244, pp258-261.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|1675 +/- 11 Ma to 1673 +/- 15 Ma.|Unit in Durlacher Supersuite.||Southeast of Howler Well, intrudes a garnet schist of the Leake Spring Metamorphics. Intrudes Rubberoid Granite and Pooranoo Metamorphics. Is unconformably overlain by Yilgatherra Formation.|Massive, medium-grained, megacrystic and porphyritic biotite(-muscovite) metamonzogranite to metasyenogranite; tabular megacrysts of K-feldspar up to 7cm long.|
31962|Pimbyana Granite|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Age derived from metatonalite sample (169054.1.pdf)|1674 Ma +/- 6 Ma (SHRIMP)|Durlacher Supersuite|||Porphyritic, biotite--muscovite granodiorite to syenogranite, with inclusions of metasedimentary and metamafic rock. Massive, medium grained porphyritic biotite monzogranite, equigranular fine-medium grained biotite tonalite and granodiorite.|
31962|Pimbyana Granite|69237|5|Briefly described|p1, p3, p12-13|||Gascoyne Province.|1773-1675 Ma.|Durlacher Supersuite.||Is intruded by the Gifford Creek Ferrocarbonatite Complex.||
31962|Pimbyana Granite|69546|5|Briefly described|p100,105,107,111|Statherian|Statherian|Geological province: Gascoyne Province. [Misspelt in Fig 6 p108 as Pymbiana Granite.] Intruded by Gifford Creek Ferrocarbonite Complex. ||Unit of Durlacher Supersuite.||||
31962|Pimbyana Granite|70127|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|1682-1619 Ma.|Durlacher Supersuite.|||Massive, medium-grained, megacrystic and porphyritic biotite(-muscovite) monzogranite; tabular megacrysts of K-feldspar up to 7cm long.|10-NOV-15
31962|Pimbyana Granite|70138|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.||Durlacher Supersuite.|||Massive, medium-grained, megacrystic and porphyritic biotite(-muscovite) monzogranite; tabular megacrysts of K-feldspar up to 7cm long.|
31962|Pimbyana Granite|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_geologysub_lut.csv, 100k_interpgeop_lut.csv, 169054.1.pdf, 178029.1.pdf|1675-1673 Ma||||Massive, medium grained, megacrystic and porphyritic biotite monzogranite. Porphyritic, medium to coarse grained biotite-muscovite granodiorite to syenogranite. Equigranular, fine to medium grained biotite tonalite and granodiorite.|
31962|Pimbyana Granite|70814|5|Briefly described|p3, p49, p70|Statherian|Statherian||1675-1660 Ma|Durlacher Supersuite||Unconformably overlain by the Edmund Group.||
31962|Pimbyana Granite|71869|5|Briefly described|p8, app p14|||Capricorn Orogen.|1673 +/- 15 Ma and 1675 +/- 11 Ma (ign. Cryst.)|Durlacher Supersuite|||Biotite monzogranite and porphyritic syenogranite.|
31962|Pimbyana Granite|74493|5|Briefly described|p3 Fig.2, p4 Fig.3, p6, p8 Fig.5, p18|||||||Cut by Gifford Creek Carbonatite Complex||
31962|Pimbyana Granite|74494|5|Briefly described|p1008-1009, p1012, p1014, p1019, p1022|Mesoproterozoic|Mesoproterozoic|Intruded and fenitised in part by ironstone dykes of the Gifford Creek Carbonatite Complex. See also p1013 Tb.1.||Durlacher Supersuite||Intruded by Gifford Creek Carbonatite Complex||
79282|Pincher Well Volcanics|68698|5|Briefly described|p27-28|||Brief geochemistry.|||||Includes felsic schist.|
78382|Pincunah Banded-Iron Member|69013|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane. Also appears as Pincunah Banded Iron Member.||Of the Kangaroo Caves Formation.|||Banded-iron-formation; jaspilitic; minor layered chert and shale; metamorphosed.|30-APR-14
78382|Pincunah Banded-Iron Member|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Age constrained by the Kangaroo Caves Formation.||Of the Kangaroo Caves Formation.|||Banded iron-formation, jaspilitic, minor layered chert and shale; metamorphosed.|05-MAY-14
78382|Pincunah Banded-Iron Member|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Kangaroo Caves Formation|||Banded iron-formation; jaspilitic; minor layered chert and shale; metamorphosed.|
78382|Pincunah Banded-Iron Member|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.|3255-3235 Ma (inferred)|Unit of Kangaroo Caves Formation.|Includes Pincunah Banded-Iron Member.||Banded iron-formation; jaspilitic; minor layered chert and shale; metamorphosed|
40752|Pincunah Monzogranite|24554|4|Described|P5 Tb.1, p8|Archean|Archean|Of the Yule Granitoid Complex. Age: c. 2945-2930 Ma. Geological Province: East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
40752|Pincunah Monzogranite|50146|5|Briefly described|Map Legend|Archean|Archean|Of the Yule Granitoid Complex. Geological Province: Pilbara Craton. Moderately to strongly feldspar (-quartz)-porphyritic biotie (-hornblende) monzogranite; weakly to moderately foliated, typically with a strong phenocryst alignment||||||07-NOV-08
40752|Pincunah Monzogranite|50379|5|Briefly described|Map Legend|Archean|Archean|Of Yule Granitoid Complex. Geological Province: Pilbara Craton.||||||07-NOV-08
40752|Pincunah Monzogranite|63441|5|Briefly described|p11 Tb. 2|Archean|Archean|Of Sisters Supersuite. Geological Province: Pilbara Craton.||||||15-APR-13
40752|Pincunah Monzogranite|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Unit in Sisters Supersuite. Feldspar(-quartz) porphyritic, (hornblende-)biotite monzogranite; weakly to moderately foliated with characteristic phenocryst alignment; minor pegmatite and leucogranite. ||||||
40752|Pincunah Monzogranite|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton. Rafts of the Pincunah Monzogranite occur within Numbana Monzogranite (Split Rock Supersuite).||Of the Sisters Supersuite.|||Feldspar(-quartz) porphyritic, (hornblende-)biotite monzogranite; weakly to moderately foliated with characteristic phenocryst alignment; minor pegmatite and leucogranite.|30-APR-14
40752|Pincunah Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Sisters Supersuite|||Feldspar(--quartz) porphyritic, (hornblende--)biotite monzogranite; weakly to moderately foliated with characteristic phenocryst alignment; minor pegmatite and leucogranite|
40752|Pincunah Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; North Pilbara Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|2954-2919 Ma (inferred)|Unit of Sisters Supersuite.|||Feldspar(-quartz) porphyritic, (hornblende-)biotite monzogranite; weakly to moderately foliated with characteristic phenocryst alignment; minor pegmatite and leucogranite|
40752|Pincunah Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
40752|Pincunah Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Sisters Supersuite|||Porphyritic biotite(-hornblende) monzogranite; feldspar and quartz phenocrysts, commonly aligned; metamorphosed.|
75573|Pindar beds|65074|4|Described|p349, p351-353, p355 Tb. 4-11|Mesoproterozoic|Mesoproterozoic|Of NW Birrindudu Basin. 300m thick. Reference area 2 km SW of northern Palm Springs, Denison Range.||||Probably equivalent to Coomarie Sandstone.|Arenite, siltstone, shale.|
75573|Pindar beds|69440|6|Mentioned|p25:2|||||||Is overlain unconformably by Denison beds.||12-JUL-16
75573|Pindar beds|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
74466|Pindinyah Formation|67202|5|Briefly described|p125|Neoproterozoic|Neoproterozoic|||Tarcunyah Group.||||
74466|Pindinyah Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||crystalline carbonate, sandstone, conglomerate|
23905|Pingandy Dolomite Member|24183|6|Mentioned|p16|||Of the Top Camp Formation. Correlated with the Devil Creek Formation.||||||
23905|Pingandy Dolomite Member|40088|6|Mentioned|p227|||||||||
23905|Pingandy Dolomite Member|40089|2|Defined|p42|Mesoproterozoic|Mesoproterozoic|||||||
22658|Pinjar Member|12759|2|Defined|p38; p28 Tb. 7; p32 Fig 15; P36 Fig 17|Aptian||New name. Named from: Lake Pinjar, Wanneroo, N of Perth. Type Section: Bore AM24, between 157-223 m depth (max 150 m). At AMG Z50, 389624 m E, 6491151 m N.||Member of Leederville Fm.||Overlain unconformably by Osborne Formation, Molecap Greensand or Gingin Chalk; underlain conformably by Wanneroo Member.|Discontinuous, interbedded sandstones, siltstones and shales of marine and non-marine origin; individual sandstone beds c.3 to 6 m thick.|12-MAY-14
22658|Pinjar Member|67115|5|Briefly described|p63-6, p70|Cretaceous|Cretaceous|Forms the upper confining layer. Lithology and trace elements detailed.||Unit in Leederville Formation.||Overlies the Wanneroo Member; is overlain by the Kardinya Shale Member and Mirrabooka Member (Osborne Formation).|Interbedded silty sandstones and shales of marine and continental origin.|
22658|Pinjar Member|68254|5|Briefly described|p1039, p1040 Tb.3, p1046 Tb.4-5|Cretaceous|Cretaceous|Identifiable by its characteristically high gamma ray logs.||Of the Leederville Formation|||Comprises micaceous and glauconitic marine siltstones and shales.|20-JUL-15
22658|Pinjar Member|68811|6|Mentioned|p180 tbl 39|Cretaceous|Cretaceous|||Of Leederville Formation.||||15-APR-20
38674|Pinjarra Granite|23788|5|Briefly described|p3 Fig. 1|||Geological Province: Yilgarn Craton.||||||
68504|Pinnacle Hill Gneiss|63441|2|Defined|p10 Tb. 2, p36|Archean|Archean|Of Railway Supersuite. Unconform. below Hardey Fm.Intruded by Cliff Pool Tonalite. Ages:3114+/-5ma, 3110+/-4Ma. Geol.prov: Pilbara Cr. Banded, grey, tonalitic gneiss, containing xenoliths of amphibolite-facies mafic gneiss and sheets of leucocratic gneiss||||||07-FEB-11
68504|Pinnacle Hill Gneiss|64174|5|Briefly described|Map legend|Archean|Archean|Of the Railway Supersuite.  Age range: 3130-3114Ma. Geological province: Sholl Terrane, West Pilbara Superterrane. Banded tonalite to granodiorite gneiss with xenoliths of amphibolite facies mafic gneiss, and sheets of leucogranitic gneiss.||||||07-NOV-08
68504|Pinnacle Hill Gneiss|64580|4|Described|map legend||Mesoarchean|Of Railway Supersuite. Banded tonalite to granodiorite gneiss with xenoliths of amphibolite facies mafic gneiss, and sheets of leucocratic gneiss.||||||15-DEC-08
68504|Pinnacle Hill Gneiss|67201|4|Described|p16-17 Fig.9, p19|Archean|Archean|In northwestern Pilbara Craton, Sholl Terrane, West Pilbara Superterrane.||Railway Supersuite||Is intruded by Cliff Pool Tonalite (Elizabeth Hill Supersuite).|Banded tonalite to granodiorite gneiss with xenoliths of amphibolite facies mafic gneiss, and sheets of leucocratic gneiss.|24-NOV-16
68504|Pinnacle Hill Gneiss|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Railway Supersuite.|||Banded tonalite to granodiorite gneiss with xenoliths of amphibolite facies mafic gneiss, and sheets of leucocratic gneiss|
68504|Pinnacle Hill Gneiss|70775|5|Briefly described|p15, p37-p38|||Sholl Terrane, Pilbara Craton. Outcrop area briefly discussed.||Railway Supersuite||Intruded by the Cliff Pool Tonalite.|Banded tonalite to granodiorite gneiss with xenoliths of amphibolite facies mafic gneiss and sheets of leucocratic gneiss.|
68504|Pinnacle Hill Gneiss|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||tonalite, felsic gneiss|
68504|Pinnacle Hill Gneiss|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||Max age 3130+/-4 Ma, min 3114+/-5 Ma.|Railway Supersuite|||Banded metatonalite and metagranodiorite gneiss; xenoliths of amphibolite and leucocratic granitic gneiss.|
78694|Pinnacles Desert Member|69788|3|Fully described|p1023, p1026 Fig.2, p1029-1035, p1037|Pleistocene|Pleistocene|New name. Type locality described. 2-6m thick. Partly retains original aragonite and high-Mg calcite mineralogy of the bioclasts. Underwent karstification after deposition of eolianite; the dissolution voids were partly filled with laminated microbialites. OSL ages by Lipar and Webb (2014): they probably represent eolian deposition of sand, followed by microbialite formation. Has best-developed karst surface; outcrops as pinnnacles for which it is named. Remnants of a paleosol surface remain.|182 +/- 23 ka and 177 +/- 30 ka.|Unit in Tamala Limestone.||Overlies Stockyard Gully Member. Is overlain by Burragenup and Vittoria Members.|Consists of an eolian calcarenite/calcrete-microbialite/paleosol cycle.|
78694|Pinnacles Desert Member|69840|4|Described|p185, p187, p190, p200, p186 Fig.3|Pleistocene|Pleistocene|See also p191 Fig.8, p196 Fig.13, p197. Dating using OSL and U/Th geochronology.  4 samples dated. Ages range from 0.207+/-0.057 Ma to 0.176+/-0.037 Ma. Marine Isotope stage 6-7.|0.17700 +/- 0.03000 Ma|Tamala Limestone||Partially overlies undivided Tamala Limestone and Nambung Member.|Microbialite. c. 5% aragonite remaining calcite.|
39348|Pinndinnis Granite|24091|4|Described|p79|Archean|Archean|Age: 2664+/-5Ma. Geological Province: Yilgarn Craton.||||||07-NOV-08
79864|Pinto Basalt|70802|5|Briefly described|250k_pre_mesozoic_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Madura Province. Events: Maralinga Event (1200-1100 Ma); Madura Province events (1900-1330 Ma).|1600 Ma; 1389+\-7 Ma||||Basalt schist intruded by plagiogranite veins and pods; may include intrusions of Moodini Supersuite|
79864|Pinto Basalt|71165|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Madura Province.|c.1400 Ma.||||Basalt schist intruded by plagiogranite veins and pods.|
79864|Pinto Basalt|72710|6|Mentioned|p4.|Statherian|Statherian|Associated with the Madura Province proto-oceanic crust and an ocean-continent transition zone.|c. 1600 Ma.||||Includes metabasaltic rocks.|
79864|Pinto Basalt|73084|4|Described|p: 15, 19, 21, 56, ~74-82, 91, 94-95...|||Madura Province. Lower amphibolite facies (peak). Oldest lithological unit in drillcores from the province inferred from relative dating relationships; interpreted to be considerably older that cross-cutting adakite of the Haig Cave Supersuite. An age of c. 1950 Ma is inferred from non-radiogenic Nd isotope composition assuming the magmatic source was uncontaminated asthenosphere melts. This assumption is generally supported by whole-rock geochemistry. Trace elements indicate a transitional source type between E-MORB and OIB; interpreted as the result of decompression melting. Distinct layered and laminated texture could suggest a tuffaceous protolith. Denoted in the aeromagnetic data by distinctive striated banding. Report includes lithologic/petrographic description, structural analysis, whole-rock geochemistry, Sm-Nd. Also p: 118-121, 126-127, 130-132, 137, 139, 141-142.||||Intruded by Haig Cage Supersuite.|Fine-grained (average 1-2 mm), variably coloured, distinctly laminated to layered, foliated mafic amphibolite schist.|
75277|Pioneer Monzogranite|65264|5|Briefly described|p25, p48 Appdx. 1|Archean|Archean|Foliated biotite monzogranite; gneiss enclaves.||||||07-FEB-11
75277|Pioneer Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Foliated biotite monzogranite; gneiss enclaves.|07-AUG-15
75277|Pioneer Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Foliated biotite monzogranite; gneiss enclaves.|
75277|Pioneer Monzogranite|70802|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton.|||||Foliated biotite monzogranite; gneiss enclaves|
75277|Pioneer Monzogranite|71270|4|Described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton.|||||Foliated biotite monzogranite; gneiss enclaves|
74833|Pirgan Monzogranite|64891|5|Briefly described|p37 Fig. 2, p52-53 Tb. 1|Archean|Archean|Of the Tuckanarra Suite. Age: c.2670Ma. Geological province: Murchison Domain. Monzogranite; metamorphosed.||||||07-FEB-11
74833|Pirgan Monzogranite|67129|5|Briefly described|p19 Fig.20|Archean|Archean|Murchison Domain, Youanmi Terrane.||Tuckanarra Suite.|||Monzogranite.|
74833|Pirgan Monzogranite|69583|6|Mentioned|p52|||Murchison Domain.||||||
74833|Pirgan Monzogranite|70796|5|Briefly described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_interpgeop_lut.csv., 500k_interpgeop_lut.csv.|ca 2690  2665 Ma (inferred)|Tuckanarra Suite|||Monzogranite; weak solidstate overprint, generally increasing towards pluton margins; metamorphosed|
74833|Pirgan Monzogranite|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.|2697-2665 Ma (inferred)|Unit of Tuckanarra Suite.|||Monzogranite; weak solid-state overprint, typically increasing towards pluton margins; metamorphosed|
77235|Pirntirri suite|66256|5|Briefly described|p8, p18 Fig.14, p24-32, see comments|Ectasian|Ectasian|Age: early Musgravian. In northeastern part of Tjuni Purlka Tectonic Zone. More texturally and compositionally homogeneous granites. Geochemistry provided. SHRIMP crystallization age. Metamorphic age: 1175+/- 10 Ma (GSWA). See also p34, p36, p38, p41, p44, p54 App.1, p66 App.3.|1217 +/- 12 to 1205 +/- 6 Ma.|Pitjantjatjara Supersuite|||Granite.|11-JAN-17
77235|Pirntirri suite|67375|5|Briefly described|p18 Fig.11, p25, p26 Fig.19. |Mesoproterozoic|Mesoproterozoic|A-type. Volcanic-arc and syn-collisional granite. Yb-enriched. Early Musgrave Orogeny. |1217-1205 Ma.|Unit in Pitjantjatjara Supersuite.||||
77235|Pirntirri suite|67553|5|Briefly described|p27-28,33|Ectasian|Ectasian|Geological province: Musgrave Province, North Australian Craton. Early Musgravian granite. Occurs in the Tjuni Purlka Tectonic Zone. Associated with high-pressure melting and low-Yb magmatism (GSWA 184146, 185610 and 187274). Oldest manifestation of the Pitjantjatjara Supersuite in the region. Two samples yielded crystallisation ages of 1217+\-12 Ma (GSWA 187166) and 1205+\-6 Ma (GSWA 187274).|1200 Ma|Unit of Pitjantjatjara Supersuite.||||
77235|Pirntirri suite|69091|4|Described|p64 Fig.4.10, p65|||Early Musgravian granite. From Tjuni Purlka Tectonic Zone (Smithies et al., 2010), which, like those of Mamut suite, are the oldest local manifestation of Pitjantjatjara Supersuite. Two samples yielded crystallisation ages of 1217 +/- 12 Ma (GSWA 187166, Kirkland et al., in prep.) and 1205 +/- 6 Ma (GSWA 187274, Kirkland et al., 2009d).|1217+/12 Ma, 1205+/-6 Ma|Pitjantjatjara Supersuite|||Granite.|
77235|Pirntirri suite|69729|5|Briefly described|p74-78|||Is presented variously as Pirntirri-Mamut suite, Mamut-Pirntirri suite and Mumut[sic]-Pirntirri suite. They are collectively described as a regional, compositionally distinctive suite, representing the earliest stages of Musgrave Orogeny magmatism in the Tjuni Purlka Zone (c.1217 Ma) and the Mamutjarra Zone (c.1200 Ma). Geochemistry plots.||Pitjantjatjara Supersuite.|||A-type granite dykes amd plutons.|
72985|Pirrilyungka Formation|64103|2|Defined|p399 Fig. 2, p400 Fig. 3, p401-404|||Formation is Fm in text. Geological Province: Officer Basin. Depositional environment in present study is shallow marine to continental, glacigene and mass flow, deep marine. See p401-404 and p406 for detailed information.||||||03-SEP-14
72985|Pirrilyungka Formation|68270|4|Described|p678,682,684,687|Cryogenian|Cryogenian|Western Officer Basin.  Type section occurs in Vines 1, lat. 26'42'05"S, long. 128'15'08"E. 1238 m (only intersected in Vines-1) thick. Glacial deposit, with evidence of deep marine mass flow/turbidite sedimentary facies in the sandstone-mudstone dominant lower Pirrilyungka. Contains poorly preserved fragments of the acritarch Cerebrosphaera buickii, a regional biostratigraphic marker that could be used for global correlation. Correlative to Sturt Tillite and equivalents. Related to Sturt glaciation.||||Overlain disconformably by Wahlgu Formation. Underlain disconformably/unconformably by Buldya Group.|Upper unit (821 m thick): diamictite and conglomerate with lesser sandstone and mudstone, including mudstone and siltstone rhythmite. Lower unit (417 m thick): interbedded sandstone and mudstone with minor diamictite.|03-JUL-19
72985|Pirrilyungka Formation|68277|6|Mentioned|p103|Neoproterozoic|Neoproterozoic|Haines et al. (2008). Officer Basin.|||||Diamictite and dropstone-bearing unit.|
72985|Pirrilyungka Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|Officer Basin.||||||
72985|Pirrilyungka Formation|69091|5|Briefly described|p43|||Western Officer Basin. Deposited during Sturt glaciation, and separating Buldya Group and Wahlgu Formation, may be present near west Musgrave Province. To date recognised only in GSWA Vines 1 drill core (Haines et al., 2008).||||Overlies Buldya Group; is overlain by Wahlgu Formation. Probably equivalent to Lupton Formation.|Monomictic and grey diamictite.|15-AUG-18
72985|Pirrilyungka Formation|73392|6|Mentioned|p4||||||||Sampled from core of GSWA Vines 1 well.|
76006|Piti Palya Metamorphics|66281|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Name reserved (Smithies 2008) as Pity Palya Metamorphics. Musgrave Province.|1360-1293 Ma.||||Pelitic and psammitic gneiss; interlayered metasiliciclastic rocks and metamorphosed volcaniclastic rocks; fine- to medium-grained quartzo-feldspathic gneiss.|
76006|Piti Palya Metamorphics|66282|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Is mapped as seven separate but un-named units of differing lithologies.|1360 - 1293 Ma.||||Undivided: weakly to strongly banded gneiss; typically quartzofeldspathic but includes amphibolitic rocks; mostly of sedimentary or volcanosedimentary protolith but possibly includes felsic to mafic intrusive protolith.|
76006|Piti Palya Metamorphics|67375|5|Briefly described|p13, p22, p75.|||Mamutjarra Zone and Tjuni Purlka Tectonic Zone, west Mulgrave Region. Displayed on the first edition BATES, BELL ROCK, BLACKSTONE and HOLT geological maps as a separate sequence from the Wirku Metamorphics. Subsequent work did not support this division, so they are now all grouped in the Wirku Metamorphics. They remain separated on all 1:100 000 scale maps published before 2011.|||||Supracrustal gneisses.|
76006|Piti Palya Metamorphics|67553|6|Mentioned|p15,23|||Geological province: Musgrave Province, North Australian Craton. Previously mapped on the first edition BATES, BELL ROCK, BLACKSTONE, and HOLT geological maps, and occurs in the Mamutjarra Zone and Tjuni Purlka Tectonic Zone. Superseded, now part of Wirku Metamorphics.||||||
76006|Piti Palya Metamorphics|70634|6|Mentioned|183595.1.pdf|Mesoproterozoic|Mesoproterozoic|Sample description(183595.1.pdf): medium grained diatexite, SHRIMP age constrains the deposition for the protolith of these metamorphic rocks. Reincorporated into the Wirku Metamorphics.|1363 Ma +/-14 Ma (SHRIMP)|||||
76006|Piti Palya Metamorphics|70793|5|Briefly described|183595.1.pdf|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province. Sample GSWA 183595 (deztexitic migmatite) yielded an interpreted maximum depositional age of 1363+\-14 Ma for the sedimentary protolith, and a high-grade metamorphic date of 1034+\-17 Ma.||||||
76006|Piti Palya Metamorphics|71268|4|Described|183595.1.pdf|Mesoproterozoic|Mesoproterozoic|Geological Province: Musgrave Province. Sample GSWA 183595 (diatexitic migmatite) yielded a weighted mean 207Pb/206Pb date of 1363+\-14 Ma, interpreted as maximum depositional age for the sedimentary protolith; and weighted mean 207Pb/206Pb age of 1211+\-33 Ma, interpreted as a high-grade metamorphic and melting event.||||||
76006|Piti Palya Metamorphics|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1363+/-14 Ma (MDA?: U-Pb zircon SHRIMP)||||Diatexitic migmatite.|
39078|Pitjantjatjara Supersuite|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes: Pottoyu Suite, Amputjuta Dacite, Manturrur and Umutju Suites, Walal Granite, Kulpitjata Suite, Ayers Range Granite, Kulgera Granite and the Umbeara granites.  Age: 1190-1120Ma. Geological Province: Musgrave Block.||||||
39078|Pitjantjatjara Supersuite|60679|5|Briefly described|Map Legend|Stenian|Stenian|Age: 1190-1120 Ma. Predominantly granites with some other similar rocks. Geological Province: Musgrave Block.||||||14-JAN-05
39078|Pitjantjatjara Supersuite|61154|2|Defined|p42 App., p9, p26-27|Mesoproterozoic|Mesoproterozoic|Comprises extensive suites of geochemically related granite bodies: Pottoyu, Umutju, and Kulpitjata Suites, Ayers Range and Kulgera Granites, Mantarurr Suite, Wala Granite(NT); and, Ernabella Adamellite suite, Ngarinya Adamellite(SA).  Age: ~1190-1120Ma.||||||03-AUG-05
39078|Pitjantjatjara Supersuite|61524|5|Briefly described|p16, p17 Fig.1, p18 Fig.2(a)|Mesoproterozoic|Mesoproterozoic|Felsic intrusives - alkali granite to diorite, almost exclusively charnockite in mapping area; undeformed to strongly deformed. Intrudes Birksgate Complex. Previously known as the Kulgara Suite. Age: 1170-1120Ma. Geological Province: Musgrave Province.||||||03-MAY-13
39078|Pitjantjatjara Supersuite|61864|5|Briefly described|p18, p19 fig 5|||Part of the basement of Musgrave Province. Associated with Musgravian Orogeny.|||||Granitic plutons; charnockitic and microgranite compositions.|
39078|Pitjantjatjara Supersuite|63224|5|Briefly described|p9||Mesoproterozoic|Elongated intrusive bodies. Geological Province: Beadell Province.||||||07-FEB-08
39078|Pitjantjatjara Supersuite|63776|6|Mentioned|p1089|Mesoproterozoic|Mesoproterozoic|Age: 1200-1140Ma. Voluminous granites.||||||
39078|Pitjantjatjara Supersuite|63864|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: c. 1155Ma or 1186-1164Ma. Charnockite; orthopyroxene-clinopyroxene metamonzogranite weakly, strongly and massively foliated. See map legend for more information.||||||
39078|Pitjantjatjara Supersuite|63866|5|Briefly described|p202, p206-p207|||Musgrave Province. Previously known as the Kulgera Supersuite.|c. 1190-1120 Ma||Includes the Pottoyu Suite, Umutju Suite, Walal Granite, Kulgera Granite, Umbeara Granite, Mantarurr Suite and the Kulpitjata Suite.||Alkali granite to diorite and extensive biotite granite gneiss.|
39078|Pitjantjatjara Supersuite|64408|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Two dates shown: 1171-1180 Ma, 1194-1215 Ma. Not clear what was dated. Subdivided into 2 named & 11 unnamed units. Geol.  Province - Musgrave Complex.||||||16-SEP-08
39078|Pitjantjatjara Supersuite|64645|5|Briefly described|p16 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: 1200 - 1140Ma. Geological Province: Musgrave Province.||||||
39078|Pitjantjatjara Supersuite|64722|5|Briefly described|Fig. 2 p3-6, p17, 27|Stenian|Stenian|Of the Musgrave Orogen. Syn- to post-tectonic. Has within-plate, A-type affinities. Subjected to amphibolite-granulite facies metamorphism.|U-Pb zircon ages of ~1200-1120 Ma.||||Granite to diorite composition.|11-APR-12
39078|Pitjantjatjara Supersuite|64745|5|Briefly described|p375, p370, p373 Fig. 3, p374 Tab.1|||Voluminous emplacement of granitic rocks: adamellite to diorite composition, commonly porphyritic. A-type granites. Age: ca. 1.12 - 1.14Ga (U-Pb SHRIMP). Geol. Prov: Musgrave Province.||||||
39078|Pitjantjatjara Supersuite|64831|5|Briefly described|p1128 Fig. 2, p1129 Fig.3|Mesoproterozoic|Mesoproterozoic|Granitoid plutons ranging from alkali granite to quartz diorite in composition; contains microgranite and charnockite bodies. Magmatism was active from ca 1200Ma to 1150Ma (SHRIMP). See also pages 1130, 1135.||||||10-FEB-09
39078|Pitjantjatjara Supersuite|65135|4|Described|p1, p6 Fig.4, p12-13, p12 Fig.8, p16-18|Stenian|Ectasian|Most abundant in the northeast of west Musgrave Complex, but only forms small plutons and dykes in the southwest. Voluminous A-type granites. Broadly charnockitic. Metamorphosed to granulite facies. Preserves rapakivi textures in low strain zones. Divided into 2 main age groups: 1219-1200 and 1190-1155 Ma. Syn- to post-tectonic. Intruded by Alcurra Dolerite.||||||
39078|Pitjantjatjara Supersuite|65376|6|Mentioned|p9 Fig.1.2. |Mesoproterozoic|Mesoproterozoic||||||Granitic rocks.|
39078|Pitjantjatjara Supersuite|65385|5|Briefly described|pS131 Tab.2, pS132|Stenian|Stenian|Synorogenic granites. Of Musgrave Province. Intruded Birksgate Complex between 1190-1120 Ma.||||||08-MAR-12
39078|Pitjantjatjara Supersuite|65693|6|Mentioned|p3 Fig.1.|||Includes mafic dykes dated c.1149 Ma.||||||
39078|Pitjantjatjara Supersuite|65833|5|Briefly described|p1, p6 Fig.4, p12 Fig.8, p12-13, p16-18|Stenian|Stenian|Voluminous A-type granites. Rapakivi textured. Primary mineralogy includes orthopyroxene, pyroxene and biotite. Syn- to post-tectonic (Musgravian Orogeny); granulite facies metamorphism. Two major episodes of magmatism and metamorphism: 1219-1200 Ma and 1190-1155 Ma. Dated granites range from 1219 +/- 12 Ma (Bodorkos et al., 2008) to 1164 +/- 10 Ma (GSWA preliminary data). Mafic dykes intrude Musgrave Complex.||||||
39078|Pitjantjatjara Supersuite|65898|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Authors separate this into 2 unnamed Early (1219-1190 Ma), 4 unnamed Late (1190-1155 Ma) units and an ungrouped ?younger unit. Metagranites and gneiss. Also misspelt on Interpreted Bedrock Geology Figure as Pitjantjatjarra Supersuite.||||||
39078|Pitjantjatjara Supersuite|65906|6|Mentioned|p3, p5|Mesoproterozoic|Mesoproterozoic|Large proportion of outcrop in Musgrave Block. Age: 1220-1140 Ma. Produced by magmatism associated with the Musgravian Orogeny. Diorite to monzonite; within-plate, A-type affinities.||||||
39078|Pitjantjatjara Supersuite|65907|5|Briefly described|p5, p10, p13, pp26-27.|||Syn- to post-tectonic granitic intrusions; A type; metamorphosed to granulite facies. Two distinct age groups, defining Early and Late Musgravian Orogeny. |c.1219-1200 Ma, and c.1190-1155 Ma.|||||
39078|Pitjantjatjara Supersuite|66256|4|Described|p4 Fig.3, p6, p8-11, p13, see comments|Stenian|Ectasian|In west Musgrave Province. Edgoose et al. (2004) grouped syn- to post-tectonic granite magmas (of Musgrave Orogeny) into Pitjantjatjara Supersuite. Supersuite can be subdivided into eight suites based on geochemical similarities within groups of similar age and limited geographical extent. All rocks have been recrystallized at granulite facies. Granite geochemistry (whole-rock geochemical, Nd and Hf isotopic analyses) provided. Geochron (SHRIMP) results for crystallisation and metamorphic ages detailed. See also  p15-18, p23 Figs.20&21, p24-32, p34-47, p53-54 App.1, p71 App.4.|||Mirturtu, Ilurpa, Walpa, Waratjarra, Pirntirri, Punuwarra, Tjuni Purlka, Kapi-Parra suites.||3 granite groups: monzodiorite to alkali-feldspar granite; locally schlieric, biotite-orthopyroxene monzogranite to syenogranite; locally derived anatectic melts - highly leucocratic sheets and veins; depleted in REE and HFSE, enriched in LILE.|11-JAN-17
39078|Pitjantjatjara Supersuite|66280|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Divided on map into early (c.1219-1190 Ma, monzodiorite; leucogranite) and late (c.1190-1155 Ma, leucogranite; syenogranite; more) Pitjantjatjara Supersuite as well as several mapped but unnamed units of metagranite and gneiss.||||||
39078|Pitjantjatjara Supersuite|66281|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province.|||||Metamonzogranites, granodiorites, metaleucogranites, metasyenogranites, mylonitic granitic rock.|
39078|Pitjantjatjara Supersuite|66282|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Metagranite and gneiss. Mapped as eleven lithologically-different but un-named units.|||||Weakly to strongly foliated metamorphosd monzogranite, syenogranite, porphyritic leucogranite, granofels, leucosyenogranite.|
39078|Pitjantjatjara Supersuite|66284|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Includes an early and a late phase, separated by Mirturtu Monzogranite; and 13 separately-mapped but un-named units.|c.1219 - 1155 Ma.||Includes Umutju Granite.||Includes metagranodiorite, metamonzogranite, gneissic porphyritic leucogranite, medium-grained mafic granulite, granitic gneiss, metasyenogranite.|
39078|Pitjantjatjara Supersuite|66526|5|Briefly described|p35.|Proterozoic|Proterozoic|Granitic rocks. They include a dated gabbro intrusion and associated mafic granulite produced in the Pitjantjatjara Event, ME 22 in the Proterozoic Mafic-Ultramafic Magmatic Event Series.|c.1180 Ma.|||||
39078|Pitjantjatjara Supersuite|67128|5|Briefly described|p5 Fig.3, p6-8, p15|||Walpa Pulka Zone, western Musgrave Province. Voluminous A-type felsic and minor mafic magmatism associated with the c.1220-1150 Ma Musgravian Orogeny.|c.1220-1150 Ma.|||Is overlain unconformably by MacDougall Formation.|Typically K-feldspar porphyritic granite plutons with ultra high-T metamorphic assemblages; local schlieric biotite-orthopyroxene leucogranites.|
39078|Pitjantjatjara Supersuite|67244|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Mapped as four separate but un-named sub-units. Informally grouped into an unnamed unit and an older 'Late Pitjantjatjara Supersuite' (1190-1150) grouping of 3 unnamed units.|>1150 Ma.||||Metagranodiorite intercalated with pelitic gneiss and olivine gabbro; mylonitic, seriate to porphyritic metagranitic rock; foliated biotite-hornblende metasyenogranite with locally abundant xenoliths of felsic gneiss.|01-MAY-15
39078|Pitjantjatjara Supersuite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Musgrave Block.|~1190-1120 Ma.|||||
39078|Pitjantjatjara Supersuite|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Mapped as no fewer than 40 separate but un-named (except for the 2 units comprising the Mirturtu Suite) units.|1220 - 1150 Ma.||Includes Mirtutu Suite.||40 mapped units of variably-metamorphosed leucogranite, granodiorite, monzogranite, syenogranite, granite, olivine gabbro, monzodiorite and charnockite; pelitic gneiss; mafic granulite.|02-DEC-13
39078|Pitjantjatjara Supersuite|67375|3|Fully described|p6,Fig.5, p15, pp26-32, p58, pp150-213.|Mesoproterozoic|Mesoproterozoic|Of Edgoose et el. (2004); formerly the Kulgera Suite of Major and Conor (1993). Incorporates all igneous rocks formed during the Musgrave Orogeny, and anatectic melts as young as 1121 +/- 11 Ma resulting from high-grade metamorphism in the late stages of the Musgrave Orogeny. Most granites are metaluminous, K-rich, A-type. Enormous amounts of granitic magma, covering half the entire Musgrave Province. Most have been metamorphosed to granulite-facies, and range from statically recrystallized and unfoliated to strongly foliated and mylonitized. Is intruded by a tubular-shaped mafic-ultramafic chonolith which hosts the world-class Nebo-Babel Ni-Cu-PGE sulfide orebody.|1219 +/- 12 Ma - 1148 +/- 6 Ma.||Includes Tjuni Purlka Suite. Encloses xenoliths and rafts of Wirku Metamorphics. Intrudes Wankanki Supersuite.||Three groups: monzodiorite to alkali-feldspar granite dykes and small plutons; schlieric biotite-orthopyroxene leucogranite veins and sheets; locally derived anatectic melts, typically with granofelsic textures. Rare leucogabbro and norite.|
39078|Pitjantjatjara Supersuite|67536|5|Briefly described|Map Legend|Ectasian|Stenian|Musgrave Block. Informally subdivided into two parts. Possibly occurs in the Beadell Province as elliptical non-magnetic to weakly magnetic intrusive bodies, some with magnetic rims and N-trending magnetic lineations.|ca. 1200 - 1175 Ma ?||||Granitoid plutons and phases of larger plutons, non-magnetic to moderately magnetic; granitoid plutons, massive to internally zoned, including intrusive charnockite, strongly magnetic.|
39078|Pitjantjatjara Supersuite|67553|4|Described|p8-9,11-12,16-17,19-20-34,39,59,61|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province, North Australian Craton. High-K granitic plutons, dominant within the Walpa Pulka Zone, and covers roughly half of the entire Musgrave Province. Calc-alkaline to alkaline calcic 'charnockitic' magmatism at 1220-1150 Ma (Close et al., 2003; and GSWA data). Based on SHRIMP U-Pb geochronology, this can subdivided into two groups,  Early and Late Musgravian granites reflecting magmatism and metamorphism c. 1220 and 1200 Ma and c. 1190 and 1155 Ma respectively. Oldest and youngest Early Musgravian granites dated at 1219+\-12 Ma (GSWA 174737) and 1157+\-9 Ma (GSWA 189254) respectively. Most granites in the Mamutjarra Zone have late Musgravian intrusive ages between 1189+\-11 Ma (GSWA 184147, Kirkland et al., 2009d) and 1148+\-6 Ma (GSWA 189522, Kirkland et al., in prep.).  Granites in the Yjuni Purlka zone include deformed early Mugsgravian granites, similar Mamutjarra Late musgravian granites and schlieric biotite-orthopyroxene leucogranites ranging from 1210+\-10 Ma (GSWA 185339, Kirkland et al., 2009e) to 1165+\-10 Ma (GSWA 183509, Kirkland et al., 2008c). Most rocks metamorphosed to granulite-facies conditions late in Musgrave Orogeny and during Giles Event. Exhumation during Petermann Orogeny exposed deep metamorphic assemblages. Subdivisible into three main lithological components (see p28-30). See also p67,70-71,73-75,78,82,95 for general field trip notes.|1220-1150 Ma||Includes Mamut, Mirtutu, Kapi-Parra, Waratjarra, Pirntirri, Ilurpa, Walpa Punuwarra and Tjuni Purlka suites.||Monzodiorite to alkali-feldspar granite, locally schlieric biotite-orthopyroxene leucogranites (monzogranite to syenogranite) and locally derived anatectic melts forming highly leucocratic sheets and veins, typically with granofelsic textures.|
39078|Pitjantjatjara Supersuite|67581|6|Mentioned|p44 Fig.8|||||||||
39078|Pitjantjatjara Supersuite|68077|5|Briefly described|p3 Fig.1, p4-6, p11-14, p18-19, p30|Mesoproterozoic|Mesoproterozoic|See also p32-38. The Musgrave Orogeny produced these extensive, >1000 oC granites. Forms a sheet up to 5km thick. Isotopic composition (Lu-Hf and Sm-Nd) and evolution tabulated and discussed in detail.|1219-1180 Ma (U-Pb zircon)||||Charnockitic and locally rapakivi-textured granites, ferroan and typically alkali-calcic; pegmatites, metagranite, metagranodiorite, monzodiorite, gabbro and dolerite.|07-SEP-17
39078|Pitjantjatjara Supersuite|68100|5|Briefly described|p2, 3, 4-5, 7-9, 12,14,15,16,24-29,33,34|Mesoproterozoic|Mesoproterozoic|Leucogranites appear as magnetic lows. Metamorphosed to granulite facies ~1080-1030 Ma (Giles Event).|1220-1150 Ma||||K-feldspar porphyritic granites and minor mafic rocks. The granites are primarily anhydrous charnockites. Anatectic, garnetiferous, mylonitic leucogranites; gabbro.|19-JAN-17
39078|Pitjantjatjara Supersuite|68131|5|Briefly described|p2 Fig.1|Mesoproterozoic|Mesoproterozoic||||||Granitic rocks.|
39078|Pitjantjatjara Supersuite|68995|5|Briefly described|p2, p5, p6, p48, p50, p51 Tb. 4, p65|Stenian|Ectasian|Intruded during the Musgrave Orogeny. Interpreted to be mostly derived from a mantle source based on isotopic concentrations and thermal limits of intrusion.|c.1220-1150 Ma|||Unconformably overlain by the Kunmarnara Group.|Orthopyroxene-bearing and locally rapikivi textured granites.|
39078|Pitjantjatjara Supersuite|68996|5|Briefly described|p3, 4, 24-25, 28-30,35-49, 54, 59|Mesoproterozoic|Mesoproterozoic|Musgrave Orogeny granites. Densities range from 2.57-3.25g/cm^3|1220-1155 Ma||||High grade granitic gneisses and charnockites. Chemistry suggests within-plate, A-type magmatism.|
39078|Pitjantjatjara Supersuite|68998|6|Mentioned|p31|||Musgrave Province. Mentioned as a significant source of zircons in the Mount Eclipse Sandstone.||||||
39078|Pitjantjatjara Supersuite|69003|5|Briefly described|p4, p37-39, p42-43, p45, p51|Mesoproterozoic|Mesoproterozoic|W Musgrave Province, Paterson Orogen. Associated with the 1220-1150 Ma Musgrave Orogeny.|1220-1150 Ma.||Tjuni Purlka suite.||Voluminous, anhydrous, orthopyroxene-bearing felsic magmatic rocks; mainly composite plutons ranging from monzodiorite through to alkali-feldspar granite, including significant rapakivi granite. Mafic rocks are extremely rare.|
39078|Pitjantjatjara Supersuite|69009|5|Briefly described|Map Legend|Stenian||Musgrave Province.|> 1078 Ma||||Comprises metagranite and gneiss.|03-APR-14
39078|Pitjantjatjara Supersuite|69091|4|Described|p52 Fig.4.1, p53, see comments|Mesoproterozoic|Mesoproterozoic|Formed during 1220-1150 Ma Musgrave Orogeny. West Musgrave Province. Mount West Orogeny and Musgrave Orogeny, including mixed with Wankanki Supersuite (Fig.4.3). In Wannarn area, Kunmarnara Group are interleaved with felsic basement, including granulite facies metagranites of Pitjantjatjara Supersuite. See also p54-56, p59 Fig.4.6, p64-67, p82-83, p85-88, p103 Fig.5.6, p105-107, p109 Fig.5.10, p113-115, p117 Fig.5.15, p119 Fig.5.16, p121, p131-132, p137-139 Figs.6.4-6.6, p141-142, p151, p183-184, p206.|1220-1150 Ma||Tjuni Purlka, Kapi-Parra, Mamut, Mirturtu, Pirntirri, Ilurpa and Waratjarra suites; Pottoyu Granite Suite.|Is unconformably overlain by Kunmarnara and Tjauwata Groups.|High-K granite plutons; most metamorphosed granulite-facies; granites range from statically recrystallised and unfoliated, to strongly foliated and mylonitised; includes high-grade granitic gneisses and charnockites; suggests A-type magmatism.|
39078|Pitjantjatjara Supersuite|69153|5|Briefly described|GEOL_LUT_CSV files;GEOCHRON/194637.1.pdf|Mesoproterozoic|Mesoproterozoic|Paterson Orogen, Musgrave Province. Some of this unit is divided into subparts: Pitjantjatjara Supersuite 1 and Pitjantjatjara Supersuite 2. Age mentioned in GEOCHRON/194637.1.pdf.|1220-1150 Ma, Smithies et al., 2010||Umutju Granite (in sub-part Pitjantjatjara Supersuite 2)||Metagranodiorite, metasyenogranite, metamonzogranite, granitic schist, granitic granofels/hornfels, mafic granulite, granitic gneiss;  intercalated with, intruded by, and included in other granitic rocks|
39078|Pitjantjatjara Supersuite|69203|5|Briefly described|p59|||Musgrave Province.|c.1190-1120 Ma.||||Voluminous I-type magmatism.|
39078|Pitjantjatjara Supersuite|69213|6|Mentioned|p36, p35|||Musgrave Province.|~1200-1140 Ma||||Anhydrous charnockites.|
39078|Pitjantjatjara Supersuite|69383|6|Mentioned|p74, 77|||Musgrave Province.|1190-1120 Ma|||||
39078|Pitjantjatjara Supersuite|69417|6|Mentioned|p2:10|Mesoproterozoic|Mesoproterozoic|Granitoids, interpreted to have formed by the extensional Musgrave Orogeny.||||||12-JUL-16
39078|Pitjantjatjara Supersuite|69436|4|Described|p21:1-2, 4-10, 15-18, 21|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Voluminous widespread syn- to post-tectonic granitic magmatism, synchronous with the Musgrave Orogeny (1220-1150 Ma). Extensively reworked by the Petermann Orogeny with pervasive biotite foliation. Peak metamorphic assemblages include biotite-epidote-muscovite +/- garnet. Three metamorphic zircon rims have ages between 574 +/- 5 Ma and 568 +/- 12 Ma. Has some potential for iron oxide-Cu-Au deposits.|1220-1120 Ma.||Pottoyu, Umutju, Mantarurr, Kulpitjata Suites; Walal, Ayers Range, Kulgera Granites.||Comprises extensive Suites of geochemically related granite bodies, from diorite to granite, generally subalkaline and predominantly ultrapotassic, although some are high-K calc-alkaline types. Metaluminous I-type.|12-JUL-16
39078|Pitjantjatjara Supersuite|69640|4|Described|p11-p12, p15, p23-p24, p27|Proterozoic|Proterozoic|Musgrave Province. Petrology, petrographic description, SHRIMP methodology, results and analayses for numerous samples are provided. Additional magmatic crystallisation ages of 1147 +/- 11 Ma,1147 +/- 16 Ma, 1143 +/- 9 Ma,  1143 +/- 8 Ma, 1155 +/- 14 Ma and 1152 +/- 9 Ma were obtained by SHRIMP. Also includes medium-grained equigranular granite with pegmatite with a rough ca 1140 Ma magmatic age and a biotite micro-syenogranite dyke dated at 1154 +/- 9 Ma. See also  p32, p50, p82, p88, p94, p100, p107, p115, p122, p130, p137, p141, p145, p148, p152, p157, p164, p174, p190, p207, p214.|1564 +/- 5 Ma (SHRIMP, magmatic crystallisation)|||Intruded by the Alcurra and Kullal dolerites. Intrudes the Birksgate Complex.|Anatectic granites, plutonic A type porphyritic granites and late crosscutting microgranitic and aplitic dykes. Porphyritic biotite monzogranite,  biotite monzogranite dykes, biotite micro-monzogranite,  monzodiorite.|
39078|Pitjantjatjara Supersuite|69655|5|Briefly described|p3, p5-p7, p9, p37|Stenian|Ectasian|See also p39, p44, p57-p58, p66, p77-p78. Musgrave Province. Musgrave Orogeny.|c. 1220-1150 Ma||||Orthopyroxene-bearing and locally rapakivi granites.|
39078|Pitjantjatjara Supersuite|69729|4|Described|p66-70, p74-78, p84-85, p87-88, p90|Mesoproterozoic|Mesoproterozoic|Edgoose et al. (2004). Musgrave Province. Emplaced during the Musgrave Orogeny. Geochemistry detailed. UHT conditions discussed.|1220-1150 Ma.|||Cross-cuts and encloses Wirku Metamorphics and Wankanki Supersuite.|Almost exclusively felsic, high-temperature, anhydrous, A-type, high-K, granulite facies metagranites.|
39078|Pitjantjatjara Supersuite|69917|5|Briefly described|p115|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Granites of  1190-1120 Ma.||||||
39078|Pitjantjatjara Supersuite|69937|5|Briefly described|vi, p7, p9, p12, p19, p22, p27, p31|||Musgrave Province. One of the sediment sources for the Amadeus Basin.|1220-1120 Ma.||||Granites.|
39078|Pitjantjatjara Supersuite|70083|6|Mentioned|p204, 206-208, 226, 229, 231-232|||Musgrave Inlier. Associated with widespread amphibolite-granulite facies metamorphism of the Musgrave Orogeny. Magnetic anomalies support a connection with contemporaneous Nornalup Complex granites (Albany-Fraser Orogen) and Teapot [Granite Complex] granites (Warumpi Province).|~1220-1140 Ma.||||Voluminous A-type felsic magmatic rocks: felsic granitoids and microgranitic dykes.|
39078|Pitjantjatjara Supersuite|70084|4|Described|p219-225,228-229|Stenian|Ectasian|Geological province: Musgrave Province, Paterson Orogen. Associated with Musgrave Orogeny, coeval with emplacement of Esperance Supersuite and Gnowangerup Fraser Dyke Suite in the Albany-Fraser Orogen. Voluminous granitic magmatism accompanied by UHT metamorphic conditions (associated with unusually thin crust and extreme geothermal gradients), and one of the largest exposed UHT belts on Earth. Granitic composition described from Smithies et al., 2011. Lies within a single, narrow, Nd and Hf-isotopic evolution band with TDM2 values within a range of 2.2-1.6 Ga, together with the Wankanki, Papulankutja and Warlawurru supersuites, reflecting reworking of juvenile crust between ca. 2.0 and 1.6 Ga (Kirkland et al., 2013a). Mid-crustal accummulation of high Th, U and K-rich granites resulted in slow post-Musgrave Orogeny thermal decline, consistent with prolonged migmatite events (Smithies et al., 2014a).|1220-1150 Ma||||Almost exclusively felsic, anhydrous, A-type granites (ferroan, typically alkali-calcic (high-K) and range in silica content from 56.8 to 78.0 wt%, with very high concentrations of both TiO2 and P2O5 and enrichments in REE, HFSE, Th, and U.|
39078|Pitjantjatjara Supersuite|70134|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province.|||||Metagranite and gneiss (section only).|
39078|Pitjantjatjara Supersuite|70338|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Part of the basement of the Musgrave Province. Seven facies are mapped separately. Lithologies are described in a little more detail.|||||Undivided: adamellite, alkali granite, diorite. Micromonzogranite to microsyenogranite; microsyenogranite; syenogranite to quartz-monzodiorite; metasyenogranite to metaquartz-monzodiorite; monzogranite to syenogranite: porphyritic or equigranular.|07-JAN-16
39078|Pitjantjatjara Supersuite|70383|6|Mentioned|p51|Stenian|Stenian|Musgrave Province. Mentioned as a possible source of zircons aged c.1178 +/- 15 Ma, extracted from the Sprigg Diamictite Member.||||||
39078|Pitjantjatjara Supersuite|70619|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province.|1219-1148 Ma||||Metagranite and gneiss.|
39078|Pitjantjatjara Supersuite|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|Musgrave Province/(Complex?), SHRIMP dates obtained from samples (file 174558.1.pdf,   194802.1.pdf)|1134Ma (SHRIMP) -   1215 Ma (SHRIMP)|Musgrave Complex|Includes Mirturtu Suite, Umutju Granite, Mirturtu Monzongranite Suite|Intruded by Warakurna Supersuite|Hornblende--biotite--pyroxene metasyenogranite and metamonzogranite, leucogabbro, quartz diorite, feldspar porphyritic charnockite.|
39078|Pitjantjatjara Supersuite|70748|6|Mentioned|p15, p50|||Musgrave Province. Similar in age to the Eyre 1 granite.||||||25-SEP-18
39078|Pitjantjatjara Supersuite|70749|5|Briefly described|p50-51|||Emplaced during the Musgrave Orogeny.|||||Widespread and voluminous felsic intrusions.|
39078|Pitjantjatjara Supersuite|70763|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Associated with the Musgrave Orogeny. Three facies are mapped separately.|1219-1148 Ma.||||Three facies mapped separately: metagranite and gneiss; hornblende-biotite metamonzogranite and biotite-hornblende metamonzogranite, both well-foliated to gneissic, garnet-bearing, locally migmatitic.|
39078|Pitjantjatjara Supersuite|70778|6|Mentioned|p21|||Musgrave Province. Emplaced during the Musgrave Orogeny.||||||
39078|Pitjantjatjara Supersuite|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma); Musgrave Orogeny (1220-1150 Ma). Sample GSWA 174558 (quartz diorite) yielded an interpreted igneous crystallisation age of 1145+\-12 Ma (weighted mean 207Pb*/206Pb*). Sample GSWA 174594 (metaleucograbbro) yielded an interpreted (weighted mean 207Pb*/206Pb*) igneous crystallisation age of 1190+\9 Ma. Sample GSWA 174736 (granofelsic metasyenogranite) yielded an interpreted (weighted mean 207Pb*/206Pb*) igneous crystallisation age of 1180+\7 Ma. Sample GSWA 174737 (foliated metamonzogranite) yielded an interpreted (weighted mean 207Pb*/206Pb*) igneous crystallisation age of 1219+\12 Ma, and metamorphic zircon rim growth at 1171+\-12 MA. Sample GSWA 174747 (metagabbro) yielded an interpreted (weighted mean 207Pb*/206Pb*) maximum igneous crystallisation age of 1205+\-24 Ma, and metamorphic zircon rim growth at 1214+\-7 Ma. Sample GSWA 180262 (mylonitic synogranite) yielded an interpreted (weighted mean 207Pb*/206Pb*) igneous crystallisation age of 1180+\-4 Ma. Sample GSWA 180270 (metamonzogranite dyke) yielded an interpreted (weighted mean 207Pb*/206Pb*) igneous crystallisation age of 1183+\-9 Ma. Sample GSWA 180860 (metamonzogranite) yielded an interpreted (concordia) igneous crystallisation age of 1159+\-13 Ma. Sample GSWA 183459 (charnockite) yielded an interpreted (weighted mean 207Pb*/206Pb*) magmatic crystallisation age of 1178+\-12 Ma. Sample GSWA 183509 (leucogranite) yielded an interpreted (weighted mean 207Pb*/206Pb*) magmatic crystallisation age of 1165+\-10 Ma. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeol_lut.csv + geochron files for more geochronological sample analyses.|1219+\-12 Ma; 1148+\-6 Ma||Includes Mirturtu Suite, Pottoyu Granite Suite, Umutju Granite Suite.|Intruded by Warakurna Supersuite. Intrudes into Wirku Metamorphics.|Mafic granulite, granitic gneiss, metasyenogranite and metamonzogranite, granulite, metagranite and gneiss, leucocratic syenogranite, metaleucosyenogranite.|
39078|Pitjantjatjara Supersuite|70826|6|Mentioned|p10|Mesoproterozoic|Mesoproterozoic|Musgrave Province. ||||||
39078|Pitjantjatjara Supersuite|70831|5|Briefly described|p1, p3-p4, p6, p9, p13-p15, p20-p21, p23|Stenian|Ectasian|Musgrave Province. Average mineralogy is discussed. Petrography of constituent samples is discussed.|c. 1220-1150 Ma||||Well-foliated to gneissic, garnet-bearing, biotite-hornlende metamonzogranites.|
39078|Pitjantjatjara Supersuite|70839|5|Briefly described|p326-327,332,334,339-341,345|Stenian|Ectasian|Geological province: Musgrave Province. Dominates the Musgrave Province in outcrop. Emplaced between c. 1.22 and 1.15 Ga during Musgrave Orogeny (Smithies et al., 2011).|c. 1220-1150 Ma|||||
39078|Pitjantjatjara Supersuite|70968|5|Briefly described|p130|||Mentioned as possible source of detrital zircons in post-Roper Group units in greater McArthur Basin.|1220-1120 Ma.|||||
39078|Pitjantjatjara Supersuite|71088|5|Briefly described|p2, p4-p5, p7, p10, p25|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Emplaced during the Musgrave Orogeny; an extensional and intracontinental event characterised by ultra-high temperatures.|1220-1150 Ma||||Granites.|
39078|Pitjantjatjara Supersuite|71143|5|Briefly described|p433,437|||Geological province: Musgrave Province. Similar age and composition to orthopyroxene- and pigeonite-bearing monzogabbro to monzodiorite rocks found from the Moodini Supersuite in the Madura Province (includes juvenile mantle input).||||||
39078|Pitjantjatjara Supersuite|71169|6|Mentioned|p82|Stenian|Ectasian|Musgrave Province. |1220-1120 Ma|||||
39078|Pitjantjatjara Supersuite|71170|5|Briefly described|xi-xii, p5-p6, p9, p42-p43|Mesoproterozoic|Mesoproterozoic|Musgrave Orogen. Emplaced at high temperatures (>900c). See also p45, p65-p67, p109, p145, p147.|1220-1150 Ma (Smithies et al, 2010)||||Charnockitic, A-type granitic rocks.|
39078|Pitjantjatjara Supersuite|71210|6|Mentioned|p4-p5, p7-p8, p21, p23, p51, p53|||Musgrave Province. See also p66-p67, p69, p78-p82, p86, p95-p97, p99, p113. Also appears as Pitjantjatjara Supergroup p8.||||Overlain by the Kunmarnara Group.||
39078|Pitjantjatjara Supersuite|71211|5|Briefly described|p6, p7 fig 1.4, p9, p24 fig 2.1|||Musgrave Province. See also p84 fig 3.1, p104, p106, p107, p136 fig 4.1 , p230. |1220-1150 Ma||||Granites.|
39078|Pitjantjatjara Supersuite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
39078|Pitjantjatjara Supersuite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma); Musgrave Orogeny (1220-1150 Ma). Metamorphosed to granulite facies, with garnet-biotite rims around zircons indicating cooling post-peak metamorphism. Sample GSWA 174558 (mesocratic quartz diorite) yielded a weighted mean 207Pb/206Pb date of 1215+\-13 Ma, interpreted as the igneous crystallization age of the quartz diorite. Sample GSWA 174594 (plagioclase leucogabbro) yielded a weighted mean 207Pb/206Pb date of 1190+\-9 Ma, interpreted as the igneous crystallization age of the leucogabbro. Sample GSWA 174736 (granofelsic metasyenogranite) yielded a weighted mean 207Pb/206Pb date of 1180+\-7 Ma, interpreted as the igneous crystallization age of the syenite. Sample GSWA 174737 (foliated monzogranite) hosts the syenite, and is dated at 1219+\-12 Ma, and contains metamorphic zircon growths at 1171+\-12 Ma. These relationships suggest that syenogranite emplacement was broadly synchronous with the high-grade metamorphic event that affected the host monzogranite. Sample GSWA 180262 (mylonitic syenogranite) yielded a weighted mean 207Pb/206Pb age of 1180+\-4 Ma, interpreted as age of igneous crystallization of the precursor syenogranite. Sample GSWA 184146 (monzogranite) yielded a concordia age of 1201+\-6 Ma, interpreted as magmatic crystallsiation age. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeol_lut.csv.|1219-1148 Ma (inferred)||Includes Permano Adamellite, Mirtutu Suite, Pottoyu Granite Suite, Umutju Granite Suite.|Overlain by Tjauwata Group.|Granite, monzogranite, monzonite, granodiorite. Includes metagranodiorite, metamonzogranite, gneissic porphyritic leucogranite, medium-grained mafic granulite, granitic gneiss, metasyenogranite.|
39078|Pitjantjatjara Supersuite|71302|5|Briefly described|p75|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province. Voluminous granitic magmatism at c. 1220-1120 Ma.||||||
39078|Pitjantjatjara Supersuite|71321|4|Described|p1-2,4-5,10,14,17-19,21,24|Stenian|Stenian|Geological province: Musgrave Province. Voluminous, felsic, A-type granitoids synchronous with, and post-dating Birksgate Complex deformation during c. 1155 Ma Musgravian Orogeny. Form several large plutonic bodies distributed over TIEYON and dominate the basement outcrop exposure of the map sheet. Plutons also show magmatic foliation as a result of Musgravian Orogeny. Also contains locally developed, ductile to brittle structures (i.e. mylonites, schistosity, and joints) which may be attributed to Neoproterozoic-Cambrian Petermann Orogeny. Broadly grouped into 3 suites based on lithology, geochemistry and field relationships; anatectic granite suite, plutonic granite suite (intrudes into anatectic suite) and microgranite dyke suite (intrudes into both anatectic and microgranite suites). See p18-22 for detailed lithological and petrographic descriptions and field relationships in outcrop. See p40-49 for detail geochemistry breakdown and analysis. Plutons emplaced between c. 1155-1143 Ma (average c. 1148.1+\-2.4 Ma). Anatectic granite suite may have been produced by melting of Birksgate Complex basement rocks. Nd isotopic analysis indicate the anatectic and porphyritic granitic suites overlap in isotopic signatures with the Birksgate Complex, while the microgranitic suite is the most evolved. Hf isotopic analysis indicate reworking of older Birksgate crust with addition of new juvenile mantle material, while the microgranite suite reflects mixing of evolved Archean source with juvenile Birksgate basement. Contains anomalous hydrothermal related Ag-REE mineralisation. See also p32-36,38,40-50,55-56,60-64,66,74.|c. 1155-1143 Ma|||Intrudes into Birksate Complex.|Adamellite; alkali granite; diorite; often porphyritic, foliated or even massive.|24-OCT-19
39078|Pitjantjatjara Supersuite|71322|5|Briefly described|p11, p26, p33|||Musgrave Province. Age range c.1220-1150 Ma, with ultra-high temperatures persisting to c.1120 Ma. Metamorphosed at 1156 +/- 9 Ma.|1219 +/- 9 Ma (SHRIMP).||||Includes charnockitic granite.|13-DEC-21
39078|Pitjantjatjara Supersuite|71415|6|Mentioned|p16|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province.||||||19-AUG-19
39078|Pitjantjatjara Supersuite|71416|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Solid geology interpretation: monzogranite to syenogranite plutons; early stage moderately to strongly magnetic, massive to weakly foliated, mainly medium-grained, equigranular to sparsely K-feldspar-phyric, commonly leucocratic; late stage strongly magnetic, massive to weakly foliated, medium- to coarse-grained, porphyritic. SHRIMP U-Pb zircon magmatic crystallisation age.|c.1150 Ma (Dutch et al., 2013).||||Porphyritic granite to monzonite, biotite and/or hornblende, rare clinopyroxene, locally inequigranular.|
39078|Pitjantjatjara Supersuite|71536|5|Briefly described|p1, p71, p73, p78|Stenian|Stenian|SHRIMP age derived from this volume and interpreted as the magmatic age of a felsic gneiss from this supersuite.|1143 +/- 9 Ma (U-Pb SHRIMP)||||Peraluminous granite derived from melting of a pre-existing sedimentary rock (probably Birksgate Complex).|
39078|Pitjantjatjara Supersuite|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1190+/-9 Ma (crystallisation: U-Pb zircon SHRIMP)||||Metamorphosed leucogabbro, metagabbro, monzogranite, pegmatite, quartz monzodiorite, syenogranite, monzonite, granite, coarse-grained leucogranite, charnockite, granoblastic garnetiferous granite, biotite-hornblende granite.|
39078|Pitjantjatjara Supersuite|71800|5|Briefly described|p29|Mesoproterozoic|Mesoproterozoic|Musgrave Province. The probable source of sediments in the Officer and Amadeus basins on the basis of geochronology.|1.22-1.15 GA|||||
39078|Pitjantjatjara Supersuite|71893|5|Briefly described|p44, p48, p51|||Musgrave Province.|ca. 1220-1120|||||
39078|Pitjantjatjara Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Musgrave Province, Paterson Orogen.|Max age 1219+/-12 Ma, min age 1148+/-6 Ma.||Includes Umutju Granite Suite, Pottoyu Granite Suite, and informal Pitjantjatjara Supersuite 1, Pitjantjatjara Supersuite 2.||Metagranite and gneiss. Mylonitic and blastomylonitic, seriate to porphyritic granitic rock. Mylonitic, medium-grained, porphyritic metamonzogranite; K-feldspar phenocrysts up to 2 cm.|
39078|Pitjantjatjara Supersuite|72094|5|Briefly described|p2, p3, p6, 12, 13, 14, p15-16|Stenian|Ectasian|Musgrave Province. Emplacement associated with Musgrave Orogeny, which metamorphosed Warlawurru, Papulankutja, Wankanki supersuites and Wirku Metamorphics to UHT (Edgoose et al., 2004; Smithies et al., 2010). Summary table of zircon geochronology on p8 Table 1 showing ages ranging from 1171+/-4 Ma to 1157+/-9 Ma.|1219-1148 Ma|||Tectonically interleaved with Kunmarnara Group along with Warlawurru Supersuite.|Metagranite and orthogneiss.|
39078|Pitjantjatjara Supersuite|72238|5|Briefly described|p36, 38|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province. Includes 1.15 Ga granites. Intruded by Amata Dolerite.|||Includes Wallaby Rock pluton, crosscut by Amata Dolerite.|||17-SEP-19
39078|Pitjantjatjara Supersuite|72242|5|Briefly described|p27|Stenian|Stenian|Geological province: Musgrave Province. Associated with Maralinga Event (including Musgrave Orogeny). Coeval with Moodini Supersuite.||||||
39078|Pitjantjatjara Supersuite|72443|5|Briefly described|p736-737, p747-748, p753, p758|Mesoproterozoic|Mesoproterozoic|Produced by the Musgrave Orogeny. Intrudes the  exposed mid-crust of the entire 1220-1150 Ma period. Interpreted to have been emplaced at temperatures of up to 1000 degrees C and coincided with a 100 Myr period of UHT metamorphism.|1220-1150 Ma||||Ferroan, alkali-calcic granites.|
39078|Pitjantjatjara Supersuite|72476|5|Briefly described|p25|||Eastern Musgrave Province.|1190-1120 Ma.||||Abundant high temperature granites.|
39078|Pitjantjatjara Supersuite|72934|6|Mentioned|p11-12|||Musgrave Province.|||||May include A-type granite intrusions.|
39078|Pitjantjatjara Supersuite|73058|5|Briefly described|p761, p769, p771 Fig.5-6, p773-776|Stenian|Ectasian|Musgrave Province. Ferroan and typically alkali-calcic granites, extreme enrichments in REE and HFSE. Intruded almost continuously throughout the Musgrave Orogeny as voluminous, high-temperature, anhydrous granites in mid-crustal regions, source dominated by new mantle additions. Hf and Nd model ages suggest mantle extraction event at c. 1900 Ma. Inferred additional significant juvenile mantle additions are masked in Hf isotope record by HFSE enriched crustal sources. Misspelt Pitjantatjara Supersuite p775. Location in text includes p772 Fig.8-9, p777 Fig.14.|c.1220-1150 Ma||||Includes orthopyroxene-bearing (charnockitic) and locally rapakivi-textured granites.|
39078|Pitjantjatjara Supersuite|73084|6|Mentioned|p12, p96, p98, p109, p124|Stenian|Ectasia|Musgrave Province. Similar in composition and age to the Moodini Supersuite and Esperance Supersuite. Part of a regionally extensive, high-temperature event named the Maralinga Event by Spaggiari et al. (2016).|1220-1150 Ma|||||
39078|Pitjantjatjara Supersuite|73177|5|Briefly described|p1100, 1114 Fig.16|||Musgrave Province.|c.1220-1120 Ma.|||||
39078|Pitjantjatjara Supersuite|73225|5|Briefly described|p21|||Eastern Musgrave Province.|c.1155-1136 Ma.||||Granites.|
39078|Pitjantjatjara Supersuite|73232|6|Mentioned|p5, p12-14|Stenian|Ectasian|Musgrave Province. [Emplaced] during the Musgravian Orogeny. Deeply weathered, gradational boundary with overlying palaeovalley infill sediments in drillholes DH1a and S22i.|c. 1220-1120 Ma|||Intrudes Birksgate Complex. Intruded by Giles Complex including Alcurra Dolerite.|Includes granitic plutons.|
39078|Pitjantjatjara Supersuite|73234|6|Mentioned|p19|Stenian|Ectasian|Musgrave Province.|1220-1140 Ma||||Includes granites.|
39078|Pitjantjatjara Supersuite|73338|6|Mentioned|piii, p7|Stenian|Ectasian|Widespread throughout the Musgrave Province. Broadly coincident with the Musgrave Orogeny. Ages are of magmatic crystallisation. Dominant interval emplaced from 1180 Ma to 1140 Ma (Close 2013).|Ranges from 1220 Ma to 1120 Ma.|||||
39078|Pitjantjatjara Supersuite|73346|6|Mentioned|p2, p5-6, p24, p26|Stenian|Ectasian|Musgrave Province; dominates the province in outcrop. Produced during the 1219-1149 Ma Musgrave Orogeny.|1219-1149 Ma||||Includes granite.|
39078|Pitjantjatjara Supersuite|73437|5|Briefly described|p151, p153|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Emplaced during Musgrave Orogeny as voluminous mantle-derived granitic magmas.|1220-1150 Ma||||Metagranite and orthogneiss.|
39078|Pitjantjatjara Supersuite|74367|6|Mentioned|p23|||Musgrave Province.||||||
81015|Pitjantjatjara Supersuite 1|70793|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma); Musgrave Orogeny (1220-1150 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv.|1219+\-12 Ma; 1198+\-5 Ma||||Charnockite; opx-cpx(-hbl) metamonzogranite and -metasyenogranite, pyroxene metamonzogranite, metasyenogranite, metagranodiroite, monzodiorite, metaleucogranite.|
81015|Pitjantjatjara Supersuite 1|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Musgrave Province, Paterson Orogen. Age inferred: ~1219 - 1195 Ma||Pitjantjatjara Supersuite. |||Metagranite and gneiss.|
81018|Pitjantjatjara Supersuite 2|70793|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma); Musgrave Orogeny (1220-1150 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyl_lut.csv.|1188; 1148+\-6 Ma||||Leucocratic syenogranite, opx(-hbl) bearing metaleucogranite, massive to weakly banded granofels, metamonzogranite, metagranodiorite.|
81018|Pitjantjatjara Supersuite 2|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Musgrave Province, Paterson Orogen. Informally subdivided into three unnamed units.Isotopic dating from two samples.|Max age 1188+/-4 Ma, min age 1148+/-6 Ma.|Pitjantjatjara Supersuite. |||Metagranite, gneiss. Mylonitic and blastomylonitic, seriate to porphyritic metagranitic rock. Metagranodiorite w intercalations/inclusions of diatexitic pelitic gneiss. Metagranodiorite intercalated with, intruded by, and included in olivine gabbro.|
38800|Plover Bore Komatiite|23926|6|Mentioned|p33 Fig. 15|||Geological Province: Yilgarn Craton.||||||
38800|Plover Bore Komatiite|23931|6|Mentioned|p200 Fig.2|||Geological Province: Yilgarn Craton.||||||
83647|Point Irwin basaltic dyke|73480|5|Briefly described|p213-214||Calymmian|Moderately dipping N-NW-striking dyke. Plagioclase 40Ar/39Ar analyses from PI1 yielded a stairstepping spectrum from ca 850 Ma to 1400 Ma. See also Point Irwin dyke. Hosted in biotite migmatite.|1454+/-8 Ma U-Pb zircon max. crystallisation age||||Microporphyritic ophitic basaltic dyke.|
75355|Point Salvation Monzogranite|66117|5|Briefly described|Map legend|Archean|Archean|Yilgarn Craton. c.2662 Ma. Biotite monzogranite; fine- to coarse-grained; seriate to K-feldspar-porphyritic; abundant leucogranitic layers and schlieren; metamorphosed. ||||||
75355|Point Salvation Monzogranite|66119|5|Briefly described|Map legend|Archean|Archean|Yilgarn Craton. c.2662 Ma. Biotite monzogranite; fine- to coarse-grained; seriate to K-feldspar-porphyritic; abundant leucogranitic layers and schlieren; metamorphosed.||||||
75355|Point Salvation Monzogranite|66121|5|Briefly described|Map legend|Archean|Archean|Yilgarn Craton. c.2664 Ma. Biotite monzogranite; fine- to coarse-grained; seriate to K-feldspar-porphyritic; abundant leucogranitic layers and schlieren; metamorphosed. ||||||
75355|Point Salvation Monzogranite|68107|5|Briefly described|p607 Fig.3, p609 Tb.1, p615 Fig.7, p618.|Neoarchean|Neoarchean|Forms the footwall of the Yamarna Shear Zone. <4 km wide; almost 90 km long. Dated using U-Pb zircon geochronology. Syntectonic; underwent dextral shear deformation while in the magmatic state and continuing into the solid state.|c. 2665-2663 Ma (Wingate et al. 2011).||||Concordant layers of homogeneous monzogranite, leucogranite, mafic schlieren and feldspar-phyric monzogranite, with decimetre-scale banding.|22-SEP-14
75355|Point Salvation Monzogranite|68186|6|Mentioned|p6|Archean|Archean|Eastern Goldfields Superterrane. Syn-kinematic.|c.2664 Ma (Pawley et al., in press).|||||
75355|Point Salvation Monzogranite|69091|6|Mentioned|p33|||Synkinematic. Located in footwall of Yamarna Shear Zone, where dextral strike-slip shearing can be constrained at c. 2664 Ma (Pawley et al. 2012)||||||
75355|Point Salvation Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Biotite monzogranite; fine- to coarse-grained; seriate to K-feldspar-porphyritic; abundant leucogranitic layers and schlieren; metamorphosed.|07-AUG-15
75355|Point Salvation Monzogranite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|See also 100k_geologyp14_lut.csv and 500k_interpgeop14_lut.csv. (SHRIMP) age derived from biotite monzogranite sample (179446.1.pdf).|2665 +/- 7 Ma - 2663 +/- 4 Ma.||||Biotite monzogranite; fine- to coarse-grained; seriate to K-feldspar-porphyritic; abundant leucogranitic layers and schlieren; metamorphosed.|
75355|Point Salvation Monzogranite|70802|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism.|2665+\-7 Ma; 2663+\-4 Ma||||Biotite monzogranite; fine- to coarse-grained; seriate to K-feldspar-porphyritic; abundant leucogranitic layers and schlieren; metamorphosed|
75355|Point Salvation Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). Sample GSWA 183149 (biotite monzogranite) yielded a concodia age of 2664+\-5 Ma, interpreted as the magmatic crystallisation age of the monzogranite. See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 100k_geologyp14_lut.csv, 500k_interpgeop_lut.csv, 2_5m_interpgeop15_lut.csv.|2665+\-7 Ma; 2663+\-4 Ma||||Biotite monzogranite; fine- to coarse-grained; seriate to K-feldspar-porphyritic; abundant leucogranitic layers and schlieren; metamorphosed|
75355|Point Salvation Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||Max age 2665+/-7 Ma. Min 2663+/-4 Ma.||||Biotite monzogranite; fine- to coarse-grained; seriate to K-feldspar-porphyritic; abundant leucogranitic layers and schlieren; metamorphosed.|
73847|Point Samson Group|24391|6|Mentioned|p8-3 Fig.2|Archean|Archean|Geological Province: Pilbara Block.||||||07-NOV-08
26849|Point Spring Sandstone|7142|6|Mentioned|p350 Fig.4.|Late Carboniferous|Late Carboniferous|Browse Basin.||||Overlies Tanmurra Formation. Is overlain by Kulshill Group?.||20-SEP-14
26849|Point Spring Sandstone|12466|5|Briefly described|p177 Fig.10.|||||||Overlies Tanmurra Formation. Is overlain by Kuriyippi Formation.||03-SEP-14
26849|Point Spring Sandstone|13194|4|Described|p389 Tb. 4-16; p382, 402 figs 4-59,-66|Upper Carboniferous|Visean|Type Section: near Point Spring 15o24'S 128o57'E. 180-380m thick outcrop, but to 880m thick subsurface. Deltaic.||Weaber Group||Overlies Burvill Formation, Tanmurra Formation (both conformably). Part equivalent to Tanmurra Formation.|Sandstone and pebbly sandstone; minor siltstone.|
26849|Point Spring Sandstone|13234|6|Mentioned|p250 Fig.2,p262 Tb.2, |||Potential reservoir.||||Overlies Tanmurra Formation offshore.||
26849|Point Spring Sandstone|13354|6|Mentioned|p375 Fig.6.|Late Carboniferous|Late Carboniferous|Overlies Tanmurra Formation and underlies Kulshill Group of the Kinmore Group.||78||||28-OCT-14
26849|Point Spring Sandstone|22663|5|Briefly described|W97 8 to 10 fig.2||Carboniferous|||||||
26849|Point Spring Sandstone|23377|6|Mentioned|p212 Fig.5||Mississippian|In the Vulcan Sub-basin.||||||23-NOV-06
26849|Point Spring Sandstone|24390|5|Briefly described|p2 Fig. 2|Carboniferous|Carboniferous|Geological Province: Bonaparte Basin.||||||
26849|Point Spring Sandstone|24569|5|Briefly described|p248 Fig. 3|Westphalian|Namurian|Of the Weaber Group. Geological Province: Petrel Sub-basin.||||||02-MAR-05
26849|Point Spring Sandstone|32648|6|Mentioned|p32|||Namurian||||||
26849|Point Spring Sandstone|32662|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
26849|Point Spring Sandstone|32663|4|Described|Table 2|||L.Carb.||||||
26849|Point Spring Sandstone|32664|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|Briefly described in notes||||||
26849|Point Spring Sandstone|32870|5|Briefly described|p48|||||||||
26849|Point Spring Sandstone|34085|6|Mentioned|Cor.chart|||Visean - Namurian||||||
26849|Point Spring Sandstone|36257|6|Mentioned|Table 2.1|||||||||
26849|Point Spring Sandstone|36551|6|Mentioned|Table 16|||||||||
26849|Point Spring Sandstone|36890|3|Fully described|p381|||||||||
26849|Point Spring Sandstone|36904|6|Mentioned|p9|||||||||
26849|Point Spring Sandstone|40301|6|Mentioned|p7|||||||||
26849|Point Spring Sandstone|40993|6|Mentioned|Fig.1|||||||||
26849|Point Spring Sandstone|41532|6|Mentioned|p292|||||||||
26849|Point Spring Sandstone|41598|5|Briefly described|p413|||Mention p412.||||||23-NOV-06
26849|Point Spring Sandstone|41839|1|Redefined|p32|||||||||
26849|Point Spring Sandstone|41864|3|Fully described|p131|Westphalian|Visean|Unit probably diachronous.||||||
26849|Point Spring Sandstone|41865|5|Briefly described|Map legend|Westphalian|late Visean|||||||
26849|Point Spring Sandstone|41867|5|Briefly described|Map legend|Westphalian|late Visean|||||||
26849|Point Spring Sandstone|42055|4|Described|Fig.1 P52|||||||||
26849|Point Spring Sandstone|42056|6|Mentioned|p96|||||||||
26849|Point Spring Sandstone|42442|3|Fully described|p13|Namurian|Visean late|||||||
26849|Point Spring Sandstone|42547|4|Described|p103|||||||||
26849|Point Spring Sandstone|42994|6|Mentioned|p48|||||||||
26849|Point Spring Sandstone|44159|6|Mentioned|Table p.38||Early Carboniferous|||||||
26849|Point Spring Sandstone|44994|6|Mentioned|Fig.6|||See also p14. Correlation.||||||23-NOV-06
26849|Point Spring Sandstone|45038|2|Defined|p.107||Carboniferous|See also Plates and Figures. Carboniferous.||||||23-NOV-06
26849|Point Spring Sandstone|45039|6|Mentioned|p7|||See also pp26,27. Laower Carboniferous.||||||23-NOV-06
26849|Point Spring Sandstone|45050|6|Mentioned|p9|||See also pp12,17,19 etc.||||||23-NOV-06
26849|Point Spring Sandstone|45063|6|Mentioned|p8|||See also pp21, 27 & Fig. 3. L.-U. Carboniferous.||||||23-NOV-06
26849|Point Spring Sandstone|45097|6|Mentioned|p19|||Refers Thomas (1971). Correlation chart||||||
26849|Point Spring Sandstone|45169|4|Described|p6|||||||||
26849|Point Spring Sandstone|48635|14|Not recorded|p.20|||See Pl.1-sh1, Pl.2-sh.2, Fig.1. Upper Carboniferous? (D/52-10,11,14,15). p.1,5,9,10,17,22,23.||||||
26849|Point Spring Sandstone|48886|14|Not recorded|Map||Early Carboniferous|Lower Carboniferous.||||||
26849|Point Spring Sandstone|50085|5|Briefly described|p2 Fig. 2|Carboniferous|Carboniferous|Geological Province: Bonaparte Basin.||||||
26849|Point Spring Sandstone|60006|5|Briefly described|Map Legend|Namurian|Namurian|Geological Province: Bonaparte Basin. Of the Weaber Group. (not recognised in Auvergne). Sandstone, conglomerate.||||||23-JUL-04
26849|Point Spring Sandstone|60364|5|Briefly described|p189|||Conformably overlies Burvill Formation. Geological Province: Bonaparte Basin.||||||11-MAY-05
26849|Point Spring Sandstone|60386|5|Briefly described|p291|Carboniferous|Carboniferous|Petrel Sub-basin.||||Unconformably overlain by Kuriyippi Formation||
26849|Point Spring Sandstone|60682|4|Described|p22 Table 5, 26|Carboniferous|Carboniferous|Of Weaber Group. Conformably overlies Burvill Formation. Previously mapped as Border Creek Formation. Max. thickness: >240m. Sandstone, conglomerate. Geological Province: Bonaparte Basin.||||||23-NOV-06
26849|Point Spring Sandstone|61023|5|Briefly described|p2 Fig. 2|Carboniferous|Carboniferous|Geological Province: Bonaparte Basin.||||||11-APR-08
26849|Point Spring Sandstone|61542|3|Fully described|p276, p277 Fig. 2, p286|Namurian|Namurian|Formerly part of Weaber Gp now revised as Wadeye Gp - as the onshore equivalent of Arco and Aquitaine Formations. Geological Province: Bonapart Basin/Petrel-Sub-basin. Sandstone and pebbly sandstone, siltstone, shale. More on interpretation included.||||||07-FEB-11
26849|Point Spring Sandstone|62837|5|Briefly described|Stratigraphic columns|Namurian|Namurian|Of the Weaber Group.  Age: ~322-~314Ma. Geological Province:  Petrel Sub-basin (offshore).||||||
26849|Point Spring Sandstone|64580|6|Mentioned|map legend|||Of Weaber Group.||||||15-DEC-08
26849|Point Spring Sandstone|64694|5|Briefly described|p234 Fig.2, p235 Fig.3, p238 Tb.1|Serpukhovian|Serpukhovian|See also p241, p245 Fig.9. Onshore Bonaparte Basin. Appears as Point Spring Formation on p242.||Unit in Weaber Group.||Overlies Burvill and Tanmurra Formations. Is overlain by Kuriyippi Formation.||
26849|Point Spring Sandstone|65331|5|Briefly described|Map legend|Bashkirian|Serpukhovian|Of Bonaparte Basin. Of Weaber Group. Age shown as Namurian. Sandstone, conglomerate.||||||19-JUL-16
26849|Point Spring Sandstone|65382|6|Mentioned|p717 App. 2|Pennsylvanian|Pennsylvanian|Bonaparte Basin. 309 Ma at top. At the boundary of the S. ybertii and D. birkheadensis palynozones.||||||
26849|Point Spring Sandstone|67195|5|Briefly described|Appendix 2|||Bonaparte Basin.|||||Includes salmon pink medium-grained sandstone.|
26849|Point Spring Sandstone|67200|5|Briefly described|app 2 p8||||||||Medium grained sandstone.|
26849|Point Spring Sandstone|69099|6|Mentioned|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian|||Weaber Group||||04-AUG-15
26849|Point Spring Sandstone|69165|6|Mentioned|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian|||Weaber Group||||
26849|Point Spring Sandstone|69451|6|Mentioned|p35:9|||Bonaparte Basin. Previously (Petroconsultants, 1989) correlated with part of the Kulshill Group equivalent rocks in the Arafura Basin.||||||12-JUL-16
26849|Point Spring Sandstone|69452|5|Briefly described|p36:9, 12, 14, 17|Pennsylvanian|Mississippian|Formerly topmost unit in Weaber Group; since assigned to Wadeye Group by Gorter et al. (2005).||Wadeye Group.||Unconformably overlies Tanmurra Formation. Lateral equivalent of Arco and Aquitaine Formations (Wadeye Group).||23-SEP-18
26849|Point Spring Sandstone|69634|5|Briefly described|500k_geologyp08_lut.csv|Carboniferous|Carboniferous|||Unit of Weaber Group.||||
26849|Point Spring Sandstone|69673|6|Mentioned|p176 fig 146, p181|Carboniferous|Carboniferous|||||Overlies Tanmurra Formation, overlain by Kuriyippi Formation||
26849|Point Spring Sandstone|70206|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Bonaparte Basin. Not recognised in map area.||Weaber Group|Includes Border Creek Member.||Sandstone, conglomerate.|
26849|Point Spring Sandstone|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Wadeye Group.|||Quartz sandstone, minor conglomerate|
24461|Point Torment Sand|36483|2|Defined|p67|Holocene|Holocene|Abuts Mowanjum Sand; locally overlies/interfingers with Doctors Creek Fm. Max. thickness: 3m. Geol.Prov: Canning Basin. Cross-laminated, X-bedded and, very locally, bioturbated, medium and coarse quartz skeletal sand, shelly sand and lihtolcastic sand.||||||07-AUG-07
24461|Point Torment Sand|37615|5|Briefly described|Table 1|||||||||
24461|Point Torment Sand|38013|6|Mentioned|p52|||||||||
22671|Poivre Formation|23768|5|Briefly described|p31, p153|Middle Miocene|Middle Miocene|Located on Barrow Island. Geological Province: Carnarvon Basin.||||||
22673|Polar Bear Formation|14227|5|Briefly described|Enclos. 2|Pliocene|Late Miocene|Presented as Polar Bear, Roysalt FMS.||||||07-FEB-11
22673|Polar Bear Formation|22769|5|Briefly described|Table1p759|Holocene|Pliocene|||||||31-AUG-09
22673|Polar Bear Formation|42959|5|Briefly described|p63|||See also Fig.3 p58||||||
22673|Polar Bear Formation|43838|6|Mentioned|p4||Tertiary|Within Redmine Group||||||12-JUL-16
22673|Polar Bear Formation|65194|5|Briefly described|p135, p136 Fig.4.37, p137|||Possibly Pliocene or younger. Sediments in Cowan Palaeovalley. Includes gypsum-bearing evaporite deposits, aeolian lunettes and dune islands.||||||
22673|Polar Bear Formation|69598|6|Mentioned|p2, p9, p10, p11 Tb.1, p29 Tb.4|Pleistocene|Pliocene|Eucla Basin. Typically no more than 10m thick. ||Redmine Group|||Sandstones, claystones and evaporites.|
74804|Polelle Group|64891|4|Described|p34 Fig. 1, p37 Fig.2, p38, p48-9 Tb. 1|Archean|Archean|Of the newly revised Murchison Supergp (Van Kranendonk 2008). Includes Meekatharra, Greensleeves and Wilgie Mia Fms. Conformable on Norie Gp; conformable below Greensleeves Fm. Age: 2800-2730Ma. Geol.prov: Murchison Domain. For lithology see Table 1.||||||07-FEB-11
74804|Polelle Group|65546|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Murchison Supergroup, Youanmi Terrane, Yilgarn Craton. Includes Wilgie Mia Formation, Greensleeves Formation and Meekatharra Formation. Age given for Meekatharra Formation (?base of Group?) as 2800-2760 Ma.||||||
74804|Polelle Group|65548|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Murchison Supergroup, Youanmi Terrane, Yilgarn Craton. Includes Wilgie Mia Formation (2752 Ma, <2969 Ma), Greensleeves Formation and Meekatharra Formation (2800-2760 Ma).||||||
74804|Polelle Group|65550|5|Briefly described|Map Legend|Archean|Archean|Of Murchison Supergroup, Narryer and Youanmi Terranes. Includes Greensleeves Formation, Meekatharra Formation and other unnamed map units.||||||18-AUG-10
74804|Polelle Group|66195|4|Described|p605, p599 Fig.2, p611 Fig.9|Neoarchean||Dominated by mafic and ultramafic rocks; also includes felsic volcanics, BIF layers, clastic sedimentary rocks.|Age ~2800 - 2740 Ma.|In Murchison Supergroup.|Includes Murrouli Basalt, Greensleeves Formation, Wilgie Mia Formation.||Dominated by mafic and ultramafic rocks; also includes felsic volcanics, BIF layers, clastic sedimentary rocks.|13-MAR-12
74804|Polelle Group|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Unit in Murchison Supergroup.|Includes Coodardy Pool, Meekatharra, Greensleeves and Wilgie Mia Formations.|||
74804|Polelle Group|67129|4|Described|p17-20, p25-27, p30, p33-42, p46,p51,p55|Archean|Archean|Murchison Domain, Youanmi Terrane. Accompanied by widespread intrusion of synvolcanic granite plutons with common c.2950 Ma xenocrystic zircons indicating authochthonous development on older crust. Linked to a major episode of mantle melting  (plume).|2800-2735 Ma|Murchison Supergroup|Wilgie Mia, Greensleeves, Meekatharra, Coodardy Formations.|Is overlain unconformably by Glen Group.|Mafic-ultramafic volcanic rocks, intermediate to felsic volcanic and volcaniclastic sedimentary rocks and banded iron formation; gabbro.|07-SEP-17
74804|Polelle Group|67130|6|Mentioned|p40 fig 38|||||||||
74804|Polelle Group|68107|6|Mentioned|p618, p619 Fig.8|Neoarchean|Neoarchean|Western Youanmi Terrane. Transition from mafic to felsic volcanism c. 2775-2760 Ma.|||Includes the Meekatharra and Greensleeves Formations.||Bimodal volcanics.|
74804|Polelle Group|68108|5|Briefly described|p628, p651 Tb.4, p652|Neoarchean|Mesoarchean|NE Murchison Domain, Youanmi Terrane. U-Pb geochronology by Van Kranendonk & Ivanic (2008).|ca. 2800-2735 Ma||||Felsic volcanics/volcaniclastics, gabbros and dolerite sills.|
74804|Polelle Group|68109|5|Briefly described|p659|Neoarchean|Mesoarchean|Murchison Domain.|ca. 2815-2710 Ma|Of the Murchison Supergroup.|||Contains intervals of BIF.|
74804|Polelle Group|68110|4|Described|p672 Fig.1, p674-5, p681, p685-p691|Neoarchean|Mesoarchean|Murchison Domain. Mis-spelt as Pollelle in Fig.2. Geochemistry and geochronology detailed, particularly a boninite - low-Ti basalt association. Suggested source from depleted plume-related mantle residue prior to subduction-related re-enrichment.|c. 2800-2733 Ma|Unit in Murchison Supergroup.|Includes Wilgie Mia, Greensleeves and Meekatharra Formations.|Overlies and intrudes Yaloginda Formation (Norie Group). Overlain by the Glen Group.|Includes mafic to ultramafic (sub-volcanic?) sills.|
74804|Polelle Group|68280|6|Mentioned|p48||||c. 2750 Ma||||Banded iron formation.|
74804|Polelle Group|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane.  Intermediate metavolcanic rock samples: 2761 +/- 6 Ma,  2755 +/- 5 Ma U-Pb zircon,  interpreted as the igneous crystallization age. From geochron file 185957.1.pdf, 185959.1.pdf.||Of Murchison Supergroup|Includes Wilgie Mia Formation, Greensleeves Formation, Meekatharra Formation, Coodardy Pool Formation and 2 unnamed units.||Metabasalt and felsic metavolcanic rock; strongly foliated to schistose; Fine to very fine grained mafic rock, undivided; metamorphosed; typically weathered.|
74804|Polelle Group|68698|5|Briefly described|p1-2, p4-5, p7-9, p11, p13, p18-19, p21|Neoarchean|Neoarchean|At least 5km thick. Widespread crustal melting of several source regions is considered responsible for volcanics erupted in the interval 2760-2753 Ma. Age range is given as c.2800-2730 Ma on p9. A rhyolite clast within a felsic volcanic breccia has a magmatic crystallisation age of 2979 +/- 3 Ma.|c.2800-2740 Ma.|Murchison Supergroup.|Coodardy, Meekatharra, Greensleeves and Wilgie Mia Formations.|Conformably overlies Norie Group. Is overlain unconformably by Glen Group. Is intruded by Cullculli and Eelya Suites.|Widespread calc-alkaline, intermediate to silicic volcanic rocks.|
74804|Polelle Group|69014|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane.||Of the Murchison Supergroup.|Includes the Meekatharra Formation.||Includes basalt and minor felsic volcanic rocks, metamorphosed; metamafic rock; shale and mudstone, metamorphosed.|01-MAY-14
74804|Polelle Group|69404|6|Mentioned|p4 Fig.4|Neoarchean|Neoarchean|Youanmi Terrane. |c. 2800 Ma|||||
74804|Polelle Group|69583|4|Described|p47, p49, p51-53, p126; Plate 2|Mesoarchean|Mesoarchean|Murchison Domain. At least 5km thick. Coeval with emplacement of Annean Supersuite.|c.2800-2740 Ma.|Murchison Supergroup.|Coodardy, Mougooderra, Meekatharra, Greensleeves, Wilgie Mia Formations.|Conformably overlies Norie Group. Is overlain unconformably by Glen Group.|BIF, quartzite.|
74804|Polelle Group|69584|5|Briefly described|p5 Fig.2, p54|Neoarchean|Neoarchean|||Murchison Supergroup|Coodardy Formation, Mougooderra Formation, Meekatharra Formation, Greensleeves Formation, Wilgie Mia Formation||Tholeiitic basalt.|
74804|Polelle Group|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Murchison Supergroup.|Coodardy, Mougooderra, Meekatherra, Greensleeves, Wilgie Mia Formations.|Overlies Norie Group. Is overlain unconformably by Glen Group.||
74804|Polelle Group|69627|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton||Murchison Supergroup|Meekatharra Formation|||
74804|Polelle Group|69628|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton||Murchison Supergroup|Greensleeves Formation, Meekatharra Formation, Coodardy Pool Formation|||
74804|Polelle Group|70020|5|Briefly described|p117-118,129|Neoarchean|Neoarchean|Geological province: Yilgarn Craton.|2800-2730 Ma||Includes Coodardy/Mougooderra, Meekatharra, Greensleeves and Wilgie Mia formations.|Overlain unconformably by Ryansville Formation/Glen Group. Underlain disconformably by Yaloginda Formation/Norie Group.||
74804|Polelle Group|70030|4|Described|p189-192,205-208|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton. Coeval with early period of felsic magmatic activity ca. 2760 Ma, which likely coincides with initial deposition of Greensleeves Formation. Early tonalite plutonism at ca. 2780 Ma during Polelle Group deposition is isolated and produces peak zircon ages at this time.|ca. 2800-2735 Ma|Unit of Murchison Supergroup.|Includes Wilgie Mia, Greensleeves, Meekatherra and Coodardy formations.|Overlain by Glen Group/Ryansville Formation. Underlain by Norie Group/Yaloginda Formation.|Mafic ultramafic volcanic rocks, intermediate to felsic volcanic and volcaniclastic rocks, and banded iron formation.|
74804|Polelle Group|70139|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.||Murchison Supergroup.|Meekatharra, Greensleeves Formations.|||
74804|Polelle Group|70226|5|Briefly described|map legends|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Carton.|2800-2735 Ma||Yalgoo Formation||Metamorphosed volcanic (mainly mafic/ultramafic) and sedimentary rocks.|16-DEC-15
74804|Polelle Group|70332|5|Briefly described|p81|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Followed the Norie Group over the Norie mantle plume (Wyman and Kerrich, 2012).|2800-2735 Ma.|||Coeval with the Narndee Igneous Complex.|Thicker (than Norie Group), and komatiite-bearing.|
74804|Polelle Group|70418|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|2800-2735 Ma.|Murchison Supergroup.|Meekatharra, Wilgie Mia Formations.|||
74804|Polelle Group|70419|6|Mentioned|p2|||Murchison Domain, Youanmi Terrane, Yilgarn Craton.||||||
74804|Polelle Group|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton. The four facies are mapped separately.|2800-2735 Ma.|Murchison Supergroup.|||Basalt, locally moderately foliated; pillowed and spherulitic (spherules to 15mm diameter) basalt; strongly sheared mafic (and minor ultramafic) schist; BIF and minor banded chert, typically granular texture. All metamorphosed.|
74804|Polelle Group|70796|4|Described|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. Affected by the Yilgarn Craton granite magmatism (3010  2600 Ma); Youanmi Terrane events (3131  2600 Ma). See also 100k_geologyl_lut.csv, 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 155568.1.pdf, 155569.1.pdf, 155572.1.pdf, 183338.1.pdf, 185920.1.pdf, 185922.1.pdf, 185926.1.pdf, 185927.1.pdf, 185928.1.pdf, 185932.1.pdf, 185957.1.pdf, 185958.1.pdf, 185959.1.pdf, 193972.1.pdf, 197420.1.pdf, 198209.1.pdf, 198295.1.pdf, 207686.1.pdf, 211101.1.pdf, Austin100_2442_stratig.pdf, Badja100_2240_stratig.pdf, Cue100_2443_stratig.pdf, Koonmarra100_2445_stratig.pdf, Madoonga100_2444_stratig.pdf, MountMagnet100_2441_stratig.pdf, Nowthanna100_2643_stratig.pdf, Reedy100_2543_stratig.pdf, Tieraco100_2545_stratig.pdf, Wynyangoo100_2542_stratig.pdf, Yalgoo100_2241_stratig.pdf. Numerous additional lithologies are discussed.|ca 2800 to 2735 Ma (inferred)|Murchison Supergroup||Intruded by the Annean Supersuite. Overlies the Yaloginda Formation. Unconformably overlain by the Mougooderra Formation.|Basalt, komatiitic basalt, felsic volcanic and volcaniclastic rocks, banded chert and banded ironformation; metamorphosed. Mafic schist and minor ultramafic schist.|
74804|Polelle Group|70826|6|Mentioned|p6 tbl 2, p8|Neoarchean|Neoarchean|Youanmi Terrane.||Murchison Supergroup||||22-APR-20
74804|Polelle Group|70830|4|Described|p5, p7-p9, p11-p12|Neoarchean|Neoarchean|See also  p14, p27-p28, p57-p58.|c. 2800-2740 Ma||Includes the Greensleeves Formation, Coodardy Pool Formation, Meekatharra Formation and the Wilgie Mia Formation.|Conformably overlies the Norie Group. Unconformably overlain by the Glen Group. Intruded by the Yalgowra Suite and Opal Gabbro.||
74804|Polelle Group|71168|4|Described|iii, p7-p8, p10, p22|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. See also  p24-p25, p40 fig 25, p52.|c. 2800-2735 Ma||Includes the Coodardy Formation, Mougooderra Formation, Meekatharra Formation, Greensleeves Formation and the Wilgie Mia Formation.|(?Dis)conformably overlies the Norie Group. Unconformably overlain by the Glen Group.||
74804|Polelle Group|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). Sample GSWA 185957 (altered intermediate metavolcanic rock) yielded a weighted mean 207Pb/206Pb date of 2761+\-6 Ma, interpreted as the igneous crystallization age. Sample GSWA 185959 ( intermediate metavolcanic rock) yielded a weighted mean 207Pb/206Pb date of 2755+\-5 Ma, interpreted as the igneous crystallization age. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv.|2800-2735 Ma|Unit of Murchison Supergroup.|Includes Coodardy Pool Formation, Greensleeves Formation, Meekatharra Formation, Wilgie Mia Formation, Yalgoo Formation.|Intruded by Eelya Suite.|Metamorphosed BIFs and minor banded chert; foliated to schistose metabasalt and metavolcanics; mafic to ultramafic schist; andesitic volcanics; basalt; fine to very-fine grained, spinefex-textured.|
74804|Polelle Group|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|2800-2760 Ma.|Murchison Supergroup.|Meekatharra, Greensleeves Formations.|||
74804|Polelle Group|71272|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. The five facies are mapped separately.|2800-2735 Ma.|Murchison Supergroup.|||Fine- to very fine-grained metabasalt; spinifex-textured metabasalt; andesitic volcanic rock, minor dacite; mafic schist with minor ultramafic schist; metamorphosed BIF and minor banded chert.|
74804|Polelle Group|71809|5|Briefly described|map legend|Archean|Archean|Yilgarn Craton, Youanmi Terrane|~2800-2735 Ma|Of Murchison Supergroup.|Includes Coodardy Pool Formation, Meekatharra Formation.|||
74804|Polelle Group|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Youanmi Terrane.|||Includes Wilgie Mia Formation, Greensleeves Formation, Meekatharra Formation, Coodardy Pool Formation and 2 unnamed units.||Metabasalt and felsic metavolcanic rock; strongly foliated to schistose. Andesitic volcanic rock; minor dacite; metamorphosed.|
74804|Polelle Group|72389|5|Briefly described|Map Legend|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Gabanintha 1:100k map sheet 2644.||Murchison Supergroup|Includes the Greensleeves Formation and the Meekatharra Formation.|||28-AUG-20
74804|Polelle Group|72491|6|Mentioned|p5 Fig.4|||Murchison Terrane, Yilgarn Craton.||||||
74804|Polelle Group|72494|5|Briefly described|p15, p17 Fig.3, p18, 28-31|||Murchison Domain, Youanmi Terrane, Yilgarn Craton. Volcanism was related to subduction, not mantle plume incubation.|>2799 +/- 2 Ma.||Meekatharra, Greensleeves, Wilgie Mia Formations.|Conformably overlies the Norie Group.||
74804|Polelle Group|73023|5|Briefly described|p1-16|Neoarchaean|Neoarchaean|Youanmi Terrane, Yilgarn Craton. P-T metamorphic conditions analysed. Metamorphosed at 2685 +/- 15 Ma: late prograde garnet growth. The article suggests metamorphism is consistent with lithospheric extension and onset of a mantle plume event across the Yilgarn Craton.|2799 +/- 2 Ma - 2734 +/- 4 Ma.|||Unconformably overlies Gossan Hill Formation. Is overlain unconformably by Mougooderra Formation.|Greenstone sequences; includes ultramafic to mafic rocks, andesitic to rhyolitic volcanic and volcaniclastic rocks, local fine-grained sedimentary rocks interbedded with BIFs, felsic volcaniclastic rocks and shale.|
74804|Polelle Group|73410|6|Mentioned|p13||||c.2800-2735 Ma.||||Mafic schists.|
74804|Polelle Group|73453|5|Briefly described|p3|Neoarchean|Neoarchean|Youanmi Terrane (Murchison).|2800-2700 Ma||||Mafic and felsic volcanics.|
74804|Polelle Group|73526|6|Mentioned|p17|Neoarchean|Neoarchean|Youanmi Terrane.|2800-2740 Ma||||Includes boninite-like rocks.|
74804|Polelle Group|73596|5|Briefly described|p1161, 1163, 1165, 1169-1170, 1172|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane.|2800-2735 Ma.|Murchison Supergroup.|Wilgie Mia, Meekatharra, Greensleeves Formations.|Overlies Norie Group. Is overlain by Glen Group. Is intruded by Lake Johnston, Mount Magnet Monzogranites; Grass Flat Gabbro, and Narndee Igneous Complex.|Komatiitic basalt, intermediate and felsic lavas, interlayered with BIF and chert. Contains boninite-like rocks and high-Mg andesites.|
23916|Pollard Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p221 Fig. 15|Late Triassic|Middle Triassic|Of Sahul Group. In figure, Fm = Formation. Geological Province: Bonaparte Basin.||||||01-MAR-10
23916|Pollard Formation|7142|6|Mentioned|p350 Fig.4.|Late Triassic|Middle Triassic|Browse Basin.||||Overlies Osprey Formation. Is overlain by Challis Formation.||
23916|Pollard Formation|13194|6|Mentioned|p386 Tb. 4-16|Carnian|Anisian|Type Section: Sahul Shoals 1 well (2355-3249m). Up to 832m thick open-marine shelf deposits.||Sahul Group||Overlies Osprey Formation (conformably). Overlain by Challis Formation (conformably).|Sandstone with interbedded shale; minor limestone.|
23916|Pollard Formation|13222|6|Mentioned|p229 Fig.2.|||||Unit in Sahul Group.||||
23916|Pollard Formation|13354|6|Mentioned|p375 Fig.6, p376 Fig.7.|Late Triassic|Middle Triassic|Bonaparte Basin. Unit of Sahul Group. Overlies Osprey Formation and underlies Challis Formation.||96||||28-OCT-14
23916|Pollard Formation|22663|5|Briefly described|AC97 1-4 Fig.4||Late Triassic|Of the Sahul Group.||||||01-MAR-10
23916|Pollard Formation|23377|6|Mentioned|p211|||In the Vulcan Sub-basin.||||||23-NOV-06
23916|Pollard Formation|23378|6|Mentioned|p180 Fig.2||Late Triassic|Of the Sahul Group. In the Vulcan Sub-basin.||||||23-NOV-06
23916|Pollard Formation|24171|5|Briefly described|p722 Fig. 3|Triassic|Triassic|Geological Province : Vulcan Sub-Basin.||||||01-MAR-10
23916|Pollard Formation|24207|5|Briefly described|p209 Fig. 5|Late Triassic|Middle Triassic|||||||
23916|Pollard Formation|41532|2|Defined|p301|Middle Triassic||||||||
23916|Pollard Formation|42053|4|Described|p37|||See also Fig.2 p29.||||||01-MAR-10
23916|Pollard Formation|42066|5|Briefly described|Fig.3 P199|||||||||
23916|Pollard Formation|42442|2|Defined|p22|Carnian|Anisian|Age: Middle to early Late Triassic (Anisian to Carnian)||||||23-NOV-06
23916|Pollard Formation|43826|6|Mentioned|Fig.2,p163||Middle Triassic|||||||01-MAR-10
23916|Pollard Formation|60634|6|Mentioned|p1168 Fig.3. |Late Triassic|Late Triassic|||Unit in Sahul Group.||Overlies Osprey Formation. Is overlain by Challis Formation.||
23916|Pollard Formation|61548|6|Mentioned|p480 Fig.3|Ladinian|Ladinian|Northern Bonaparte Basin.||||||
23916|Pollard Formation|61550|6|Mentioned|p495 Fig.2. |Late Triassic|Late Triassic|||Unit in Sahul Group.||Overlies Osprey Formation. Is overlain by Challis Formation.||
23916|Pollard Formation|62837|5|Briefly described|Stratigraphic columns|Middle Triassic|Early Triassic|Of the Sahul Group.  Age: >240->230Ma. Geological Province:  Ashmore Platform, Vulcan Sub-basin, Londonderry High (all in Western Bonaparte Basin) and Sahul Platform (Northern Bonaparte Basin).||||||01-MAR-10
23916|Pollard Formation|63358|5|Briefly described|p4 Fig. 1.3|Carnian|Anisian|||||||01-MAR-10
23916|Pollard Formation|63929|6|Mentioned|p131 Fig.2.|Late Triassic|Middle Triassic|Ashmore Platform (east), Sahul Platform. Includes marine and non-marine sediments. Has a carbonate member at its base correlated with near the top of Locker Shale; represents a major marine highstand event across the North West Shelf.||||Overlies Osprey Formation. Is overlain by Challis Formation.||
23916|Pollard Formation|64689|6|Mentioned|p13 Fig.13|||||||Is overlain by Challis Formation, appears to overlie Mount Goodwin Limestone||
23916|Pollard Formation|66124|5|Briefly described|p171 Fig.2|Carnian|Anisian|Ashmore Platform (East). Marine. Underlies Challis Formation and overlies Osprey Formation.||||||17-AUG-18
23916|Pollard Formation|66187|5|Briefly described|p413 Fig.2|Late Triassic||Sahul Group. Underlies the Challis Formation, overlies the Osprey Formation. Mount Ashmore Dome.||||||
23916|Pollard Formation|67370|6|Mentioned|p313 Fig.2. |Triassic|Triassic|||||Overlies Osprey Formation.||
23916|Pollard Formation|68223|6|Mentioned|p178 Fig.3|Ladian|Ladian|||||||
23916|Pollard Formation|69297|6|Mentioned|p305|Carnian|Ladinian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin. ||Sahul Group||Overlies the Osprey Formation. Overlain by the Challis Formation.|Sandstone and siltstone.|
23916|Pollard Formation|69452|5|Briefly described|p36:15, 21|Triassic|Triassic|Bonaparte Basin.||Sahul Group.||Equivalent to upper part of Cape Londonderry Formation.||12-JUL-16
23916|Pollard Formation|69689|6|Mentioned|p16|Triassic|Triassic|Browse, Bonaparte Basins.||||||
23916|Pollard Formation|70061|5|Briefly described|Regional geology Fig.6-7.Vulcan Fig.2,p2|Norian|Anisian|||Sahul Group.||Overlies Osprey Formation. Is overlain by Challis Formation.||12-JUL-16
23916|Pollard Formation|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Norian|Ladinian|See also Northern: Fig.2. Yampi: Fig.2. Caswell-Barcoo Sub-basins, Browse Basin.||Sahul Group.||Overlies Osprey Formation. Is overlain by Challis Formation.||12-JUL-16
80071|Ponton Creek psammitic gneiss|69595|5|Briefly described|p10 tbl 2, p15, p16 tbl 3, p18, |Statherian|Statherian|Informal name. Shown as Ponton Creek gneiss on p57. Moderate energy, potentially shallow marine depositional environment.  Ages of inherited detrital zircons given (see page 19).See also p19, p32 fig 17, p35.|1689 +/- 6 Ma - 1666 +/- 12 Ma||||Sand and grit.|22-SEP-17
80071|Ponton Creek psammitic gneiss|70090|4|Described|p445-449,451-453,457|Statherian|Statherian|Geological province: Biranup Zone, Albany-Fraser Orogen, West Australian Craton. Of Barren Basin. Mafic magmatism associated with Biranup Orogeny. Depositional environment: moderate energy. Shallow marine? Proximal volcanics? Sedimentary protoliths deposited between 1710 Ma and 1650 Ma during Biranup Orogeny. Metamorphosed to amphibolite to granulite facies. Maximum depositional age: c. 1689+\-6 Ma. Minimum depositional age: contrained by c. 1666+\-12 Ma intrusive monzogranite. Unimodal zircon age component of c. 1690 Ma (volcanic protolith?) indicates EHfi array of -6 to 0, corresponding to 2.4-2.6 Ga model ages. Late Paleoproterozoic detrital age components suggest derivation from local Biranup Zone sources. Shown as Ponton Creek psammitic gneiss p445, 446, 447, 448, 449, 451, 453, 457.|||||Sand and grit-dominated psammitic gneiss.|08-AUG-19
80071|Ponton Creek psammitic gneiss|70182|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|Deposition was coincident with the Biranup Orogeny. Also appears as Ponton Creek Gneiss.|Between 1710 Ma and 1650 Ma.|||||
35231|Poocatche Monzogranite|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Of  Carlindi Granitoid Complex.  Geological Province: Pilbara Craton.||||||07-NOV-08
35231|Poocatche Monzogranite|24110|5|Briefly described|Plate 1|Archean|Archean|Belongs to Carlindi Granitoid Complex.  Geological Province: Pilbara Craton||||||07-NOV-08
35231|Poocatche Monzogranite|24166|4|Described|p19|Archean|Archean|Parent: Carlindi Granitoid Complex.   Intrudes the Minnamonica Monzogranite||||||07-NOV-08
35231|Poocatche Monzogranite|24193|5|Briefly described|p878 Tb.1|Archean|Archean|Geological Province: Pilbara Craton. Within the Carlindi granitoid complex. Age: ca.2890-2830 Ma.||||||07-NOV-08
35231|Poocatche Monzogranite|24327|5|Briefly described|Map Legend|Archean|Archean|Muscovite-biotite monzogranite.  Parent: Carlindi Granitoid Complex.   Age: c.2940Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
35231|Poocatche Monzogranite|24349|5|Briefly described|Map legend|Archean|Archean|Of Carlindi Granitoid Complex.   Age: c.2940Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
35231|Poocatche Monzogranite|50379|5|Briefly described|Map Legend|Archean|Archean|Of Carlindi Granitoid Complex. Geological Province: Pilbara Craton.||||||07-NOV-08
35231|Poocatche Monzogranite|63420|5|Briefly described|Map legend|Archean|Archean|Of Split Rock Supersuite. Geological Province: Pilbara Craton. Muscovite-biotite monzogranite; seriate to porphyritic; fine- to medium-grained, massive to weakly foliated; locally abundant pegmatite.||||||07-NOV-08
35231|Poocatche Monzogranite|63441|5|Briefly described|p12 tb. 2|Archean|Archean|Of Split Rock Supersuite. Geological province: Pilbara Craton.||||||07-FEB-11
35231|Poocatche Monzogranite|66108|5|Briefly described|Map legend|Neoarchean|Neoarchean|Unit in Split Rock Supersuite. Muscovite-biotite monzogranite; seriate to porphyritic; massive to weakly foliated; locally abundant pegmatite.||||||
35231|Poocatche Monzogranite|68283|5|Briefly described|Map Legend|Archean|Archean|Pilbara Craton.||Of the Split Rock Supersuite.|||Muscovite-biotite monzogranite; seriate to porphyritic; massive to weakly foliated; locally abundant pegmatite.|23-SEP-13
35231|Poocatche Monzogranite|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton. Age constrained by the parent Split Rock Supersuite.||Of the Split Rock Supersuite.|||Muscovite-biotite monzogranite; seriate to porphyritic; massive to weakly foliated; locally abundant pegmatite.|30-APR-14
35231|Poocatche Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Muscovite--biotite monzogranite; seriate to porphyritic; massive to weakly foliated; locally abundant pegmatite.|
35231|Poocatche Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; Split Rock Supersuite Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|2851-2831 Ma (inferred)|Unit of Split Rock Supersuite.|||Muscovite-biotite monzogranite; seriate to porphyritic; massive to weakly foliated; locally abundant pegmatite|
35231|Poocatche Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
35231|Poocatche Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Muscovite--biotite monzogranite; seriate to porphyritic; massive to weakly foliated; locally abundant pegmatite.|
27680|Poole Sandstone|7433|4|Described|p25 Fig.2, p32 Fig.8, pp35-36, pp52-53.|Permian|Permian|Gregory Sub-basin, Canning Basin. Shallow marine-lagoonal sandy clastics. Relatively uniform thickness of 100-200m throughout the Basin. Excellent aquifer with basin-wide extent; confined by Noonkanbah Formation. Possible coal prospectivity.||||Overlies Grant Group; unconformably in the Fitzroy Sub-basin, conformably elsewhere. Is overlain by Noonkanbah Formation.|Leached, well-sorted quartz sandstone; minor patchy white to grey silcrete.|
27680|Poole Sandstone|13255|6|Mentioned|p369|Permian|Permian|Roebuck Basin. Early Permian.||||Overlies Upper Grant Group. Is overlain by Noonkanbah Formation.||19-MAR-20
27680|Poole Sandstone|13354|6|Mentioned|p376 Fig.7.|Early Permian|Early Permian|Onshore Canning Basin. Separated from underlying Upper Grant Group by an unconformity of Sakmarian age. Underlies Noonkanbah Formation.||135||||28-OCT-14
27680|Poole Sandstone|22718|5|Briefly described|p5, Table1 p7|Artinskian|Sakmarian|||||||19-MAR-20
27680|Poole Sandstone|22738|4|Described|10,12,13,16, map|Early Permian|Early Permian|Max thickness 85 m. Overain by Wallal Sandstone, Noonkanbah Formation; underlain by Grant Group.||||||13-NOV-07
27680|Poole Sandstone|22741|5|Briefly described|p27, Table3 p13||Permian|||||||19-MAR-20
27680|Poole Sandstone|22753|5|Briefly described|Fig.3 p585|Permian|Permian|||||||
27680|Poole Sandstone|22764|4|Described|Table2,p10||Early Permian|100 m. Disconformable on Grant Formation; conformable beneath Nookanbah Formation||||||01-FEB-10
27680|Poole Sandstone|22765|5|Briefly described|p10, Table1|Artinskian|Sakmarian|||||||19-MAR-20
27680|Poole Sandstone|22767|5|Briefly described|Table3 p16, p21||Early Permian|||||||19-MAR-20
27680|Poole Sandstone|22776|6|Mentioned|Table.3|Early Permian|Early Permian|||||||
27680|Poole Sandstone|22801|5|Briefly described|p11, Table1 p9||Artinskian|||||||19-MAR-20
27680|Poole Sandstone|22814|5|Briefly described|fig2|Permian|Permian|||||||
27680|Poole Sandstone|23212|4|Described|Table.1 p7||Sakmarian|||||||
27680|Poole Sandstone|23523|5|Briefly described|p994 Fig. 2|Permian|Permian|||||||
27680|Poole Sandstone|23575|5|Briefly described|Map Legend|Permian|Permian|||||||
27680|Poole Sandstone|23745|4|Described|p19|Early Permian|Early Permian|Geological Province: Canning Basin.||||||
27680|Poole Sandstone|23765|5|Briefly described|Map Legend|Permian|Permian|||||||
27680|Poole Sandstone|23766|4|Described|p14 Tb. 2|Early Permian|Early Permian|Comprised of sandstone and siltstone. Thickness: 133m.  See also p19.||||||11-APR-08
27680|Poole Sandstone|23815|6|Mentioned|p281|Sakmarian|Sakmarian|Geological Province: Canning Basin.||||||27-APR-05
27680|Poole Sandstone|24025|5|Briefly described|p16|Early Permian|Early Permian|Geological Province: Canning Basin.||||||
27680|Poole Sandstone|24061|4|Described|p182|Early Permian|Early Permian|Geological Province:  Canning Basin.||||||
27680|Poole Sandstone|24062|5|Briefly described|p186 Table 1|Permian|Permian|Geological Province: Canning Basin.||||||
27680|Poole Sandstone|24246|5|Briefly described|p9, 14|Permian|Permian|Geological Province: Canning Basin.||||||24-FEB-05
27680|Poole Sandstone|24390|5|Briefly described|p6 Fig. 4|Permian|Permian|Geological Province: Canning Basin.  See also p8.||||||
27680|Poole Sandstone|24466|4|Described|p367|Early Permian|Early Permian|||||||
27680|Poole Sandstone|29548|6|Mentioned|p224|||||||||
27680|Poole Sandstone|29813|6|Mentioned|p7|||||||||
27680|Poole Sandstone|29817|5|Briefly described|p8|||||||||
27680|Poole Sandstone|29818|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|29819|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|30110|6|Mentioned|p81|||See also P83. Lower Permian, Artinskian age.||||||
27680|Poole Sandstone|30313|6|Mentioned|p54|||See also P55. Lower Permian age.||||||
27680|Poole Sandstone|30338|6|Mentioned|p100|||||||||
27680|Poole Sandstone|30342|6|Mentioned|p103|||||||||
27680|Poole Sandstone|30525|6|Mentioned|Map legend|Artinskian|Artinskian|||||||
27680|Poole Sandstone|30533|4|Described|p25|||On Table 7||||||
27680|Poole Sandstone|30545|6|Mentioned|Fig.2|||Sakmarian. See also P22||||||
27680|Poole Sandstone|30595|5|Briefly described|p3|||||||||
27680|Poole Sandstone|30897|6|Mentioned|p19|||Refers Guppy et al.(1958)||||||
27680|Poole Sandstone|31037|6|Mentioned|p1042|||Occurence of Metalogoceras striatem||||||
27680|Poole Sandstone|31706|6|Mentioned|p657|||Permian correlation chart||||||
27680|Poole Sandstone|32113|6|Mentioned|p52|||||||||
27680|Poole Sandstone|32376|6|Mentioned|p1541|||||||||
27680|Poole Sandstone|32648|6|Mentioned|p32|||L.Permian||||||
27680|Poole Sandstone|32945|6|Mentioned|p73|||See also P88. Sakmarian||||||
27680|Poole Sandstone|33518|4|Described|Table 1|||||||||
27680|Poole Sandstone|33519|6|Mentioned|Map legend|Permian|Permian|||||||
27680|Poole Sandstone|33701|6|Mentioned|Fig.1|||Artinskian.||||||
27680|Poole Sandstone|33960|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|33965|4|Described|Table 1|||||||||
27680|Poole Sandstone|33966|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|34138|6|Mentioned|Cor.Chart|||Sakmarian - Artinskian||||||
27680|Poole Sandstone|34287|6|Mentioned|p125|||||||||
27680|Poole Sandstone|34532|6|Mentioned|p220|||See also PP221,225. Sakmar. - Artinsk.||||||
27680|Poole Sandstone|34568|6|Mentioned|p220|||Fauna||||||
27680|Poole Sandstone|35120|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|35124|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|35127|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|35201|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|35202|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|35205|6|Mentioned|Map legend|Permian|Permian|||||||
27680|Poole Sandstone|35207|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|35222|4|Described|Table.2|||||||||
27680|Poole Sandstone|35223|4|Described|Table.2|||||||||
27680|Poole Sandstone|35225|4|Described|Table 1|||||||||
27680|Poole Sandstone|35226|4|Described|Table 1|||||||||
27680|Poole Sandstone|35250|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|35251|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|35252|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|35275|6|Mentioned|Fig.5.|||||||||
27680|Poole Sandstone|35492|6|Mentioned|p145|||||||||
27680|Poole Sandstone|35497|4|Described|Table 1|||Also on p10||||||19-MAR-20
27680|Poole Sandstone|35530|6|Mentioned|p14|||Location of Bivalvia fossils.||||||
27680|Poole Sandstone|35903|4|Described|Table 1|||||||||
27680|Poole Sandstone|35983|6|Mentioned|Table 28|||||||||
27680|Poole Sandstone|36020|6|Mentioned|p388|||||||||
27680|Poole Sandstone|36224|5|Briefly described|Map legend|Early Permian|Early Permian|Includes: Tuckfield and Nura Nura Members.  Sandstone, mudstone.||||||01-FEB-05
27680|Poole Sandstone|36225|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|36257|6|Mentioned|Table 2.1|||||||||
27680|Poole Sandstone|36438|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|36596|6|Mentioned|Text Fig.5|||||||||
27680|Poole Sandstone|36632|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|36634|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|36890|3|Fully described|p340|||Formerly Poole Range Group.||||||13-NOV-07
27680|Poole Sandstone|37106|5|Briefly described|p277|||||||||
27680|Poole Sandstone|37294|6|Mentioned|p104|||||||||
27680|Poole Sandstone|37369|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|37370|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|37549|6|Mentioned|p116|||||||||
27680|Poole Sandstone|37914|6|Mentioned|p449|||||||||
27680|Poole Sandstone|38217|5|Briefly described|p269|||||||||
27680|Poole Sandstone|38586|6|Mentioned|p29|||||||||
27680|Poole Sandstone|38603|6|Mentioned|p81|||||||||
27680|Poole Sandstone|38878|6|Mentioned|Map legend|Artinskian|Sakmarian|Sakmarian - Artinskian||||||
27680|Poole Sandstone|38886|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|38917|6|Mentioned|p169|||||||||
27680|Poole Sandstone|39796|6|Mentioned|Map legend|Permian|Permian|||||||
27680|Poole Sandstone|39857|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|40045|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|40078|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|40306|6|Mentioned|p58|||||||||
27680|Poole Sandstone|40794|6|Mentioned|p91|||||||||
27680|Poole Sandstone|40838|6|Mentioned|p281|||||||||
27680|Poole Sandstone|40992|6|Mentioned|Fig.11|||||||||
27680|Poole Sandstone|41044|6|Mentioned|p132|||||||||
27680|Poole Sandstone|41053|6|Mentioned|p98|||||||||
27680|Poole Sandstone|41100|6|Mentioned|Fig.8|||||||||
27680|Poole Sandstone|41158|6|Mentioned|p162|||||||||
27680|Poole Sandstone|41169|6|Mentioned|p148|||See also Fig.3||||||
27680|Poole Sandstone|41315|6|Mentioned|p155|||||||||
27680|Poole Sandstone|41449|5|Briefly described|p256|||||||||
27680|Poole Sandstone|41514|6|Mentioned|p68|||||||||
27680|Poole Sandstone|41632|6|Mentioned|p4|||||||||
27680|Poole Sandstone|41688|5|Briefly described|Table 4|||||||||
27680|Poole Sandstone|41689|6|Mentioned|Table 1|||||||||
27680|Poole Sandstone|41730|6|Mentioned|p483|||||||||
27680|Poole Sandstone|41828|6|Mentioned|p505|||||||||
27680|Poole Sandstone|41839|6|Mentioned|p25|||||||||
27680|Poole Sandstone|42017|6|Mentioned|p1|||||||||
27680|Poole Sandstone|42347|6|Mentioned|Fig.2 P1020|||||||||
27680|Poole Sandstone|42540|6|Mentioned|p316|||||||||
27680|Poole Sandstone|42571|5|Briefly described|p20, Table1 p9|||||||||
27680|Poole Sandstone|42572|5|Briefly described|Map Legend|Permian||||||||23-DEC-09
27680|Poole Sandstone|42613|1|Redefined|P 14, 16|||Includes "Cuncudgerie Sandstone".||||||
27680|Poole Sandstone|42710|5|Briefly described|map legend|Permian||||||||
27680|Poole Sandstone|42734|5|Briefly described|map legend|Permian||||||||
27680|Poole Sandstone|42811|5|Briefly described|p44|||||||||
27680|Poole Sandstone|42880|5|Briefly described|Fig.2,p1020|||||||||
27680|Poole Sandstone|42930|5|Briefly described|Fig.1 p473|Permian|Early Permian|Unconformably overlies Grant Formation; unconformably underlies Noonkanbah Formation. Geological Province: Canning Basin.||||||03-FEB-10
27680|Poole Sandstone|42994|6|Mentioned|p76|||||||||
27680|Poole Sandstone|43015|5|Briefly described|Table 1,p319|||||||||
27680|Poole Sandstone|43018|5|Briefly described|Table 1,p386|||||||||
27680|Poole Sandstone|43050|5|Briefly described|p16|||||||||
27680|Poole Sandstone|43173|5|Briefly described|12-54||Early Permian|||||||
27680|Poole Sandstone|43281|5|Briefly described|Map legend||Permian|||||||
27680|Poole Sandstone|43474|14|Not recorded|p71|||||||||
27680|Poole Sandstone|43563|6|Mentioned|Fig.2,p5|Artinskian|Sakmarian|||||||
27680|Poole Sandstone|43656|6|Mentioned|Fig.2,p8|Artinskian|Sakmarian|||||||
27680|Poole Sandstone|43666|6|Mentioned|p9|||||||||
27680|Poole Sandstone|43746|6|Mentioned|Fig.2,p11|Artinskian|Sakmarian|||||||
27680|Poole Sandstone|43815|6|Mentioned|p93||Permian|||||||
27680|Poole Sandstone|43816|6|Mentioned|Fig.2,p88|||||||||
27680|Poole Sandstone|43818|6|Mentioned|Fig.2.p39||Early Permian|||||||
27680|Poole Sandstone|43823|6|Mentioned|p755,Fig.2,|||||||||
27680|Poole Sandstone|43932|4|Described|p8,Tb.1 p6||Permian|||||||
27680|Poole Sandstone|44040|14|Not recorded|p41,43|||||||||
27680|Poole Sandstone|44143|4|Described|p436 Tb.4-19, p445-447|Permian|Permian|Up to 350m thick; sandstone and siltstone; shallow water, fluvial and marine. Unconformably (in Fitzroy Trough) or disconformably (elsewhere) overlies Paterson Formation and Grant Group. Type section southeastern Grant Range (MOUNT ANDERSON: 18deg 04' 30" S, 124deg 08' 30" E). Diverse fauna and flora.||||||24-NOV-17
27680|Poole Sandstone|44189|5|Briefly described|Map legend||Permian|||||||
27680|Poole Sandstone|44219|14|Not recorded|p31|Artinskian|Sakmarian|Inc. Nura Nura Member.||||||
27680|Poole Sandstone|44356|5|Briefly described|p9,Tb.1 p6|||||||||
27680|Poole Sandstone|44357|4|Described|p12,Tb.1 p9||Artinskian|Crops out SW corner of sheet area. Formerly known as the Cuncudgerie Sandstone.||||||
27680|Poole Sandstone|44403|2|Defined|p.6,8,9,11,12|||E/51-12, See Casey J.N. 1958b. for more detail.||||||
27680|Poole Sandstone|44404|14|Not recorded|map legend||Permian|||||||
27680|Poole Sandstone|44443|5|Briefly described|map legend|Early Permian|Early Permian|||||||
27680|Poole Sandstone|44479|2|Defined|Tb.1|||E/51-1. Partly correlated with the Cuncudgerie Sandstone of this Sheet.||||||
27680|Poole Sandstone|44994|6|Mentioned|p13|||||||||
27680|Poole Sandstone|44998|2|Defined|p78-9|||Defined? Lies between Grant Formation below and Noonkanbah Formation above. See also p67,70-2,83-4,103-4,131,143,221-9,245-6, App.2 p267, App.4 p 288.||||||10-FEB-20
27680|Poole Sandstone|45001|14|Not recorded|p7|Artinskian|Sakmarian|||||||
27680|Poole Sandstone|45016|14|Not recorded|p.112|||||||||
27680|Poole Sandstone|45031|14|Not recorded|p31|||||||||
27680|Poole Sandstone|45140|5|Briefly described|p67|Permian|Permian|Canning Basin. Largely fluvial deposits.||||Conformably overlies Grant Formation. Is overlain conformably by Noonkanbah Formation.||
27680|Poole Sandstone|45153|2|Defined|App.4-66|Early Permian|Early Permian|Formerly Poole Range beds.||||||13-NOV-07
27680|Poole Sandstone|45158|3|Fully described|p20|||||||||
27680|Poole Sandstone|45168|6|Mentioned|p6|||||||||
27680|Poole Sandstone|46319|4|Described|p17|Early Permian|Early Permian|Originally named "Cungudgerie Sandstone".||||||
27680|Poole Sandstone|46849|6|Mentioned|p186|||||||||
27680|Poole Sandstone|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
27680|Poole Sandstone|48573|2|Defined|p.3,8,11-14,21.|||(E51-7/Alexander Creek)||||||
27680|Poole Sandstone|48596|14|Not recorded|p.5|||(E51-11)||||||
27680|Poole Sandstone|48826|14|Not recorded|p.21|||Formation not found.||||||
27680|Poole Sandstone|48831|14|Not recorded|p.22,54,57,65|||||||||
27680|Poole Sandstone|48837|14|Not recorded|p.1|||||||||
27680|Poole Sandstone|48848|14|Not recorded|p.96,101|||||||||
27680|Poole Sandstone|49644|5|Briefly described|Table|||||||||
27680|Poole Sandstone|50085|5|Briefly described|p6 Fig. 4|Permian|Permian|Geological Province: Canning Basin.||||||
27680|Poole Sandstone|50544|5|Briefly described|p63|Sakmarian|Sakmarian|Red to yellow-brown, fine to coarse-grained sandstone with lenses of white claystone and siltstone and thin beds of matrix-supported pebble conglomerate.  Age: Early Sakmarian.  Geological Province: Canning and Northern Carnarvon Basins.||||||11-DEC-06
27680|Poole Sandstone|50555|5|Briefly described|Map legend|Permian|Permian|Fine to coarse-grained sandstone with siltstone interbeds; minor mudstone, trace fossils. Geological Province: Canning Basin.||||||03-FEB-10
27680|Poole Sandstone|60386|6|Mentioned|p297, 309|Artinskian|Artinskian|Onshore Canning Basin. Deltaic - nearshore - shelf. ||||||
27680|Poole Sandstone|61021|5|Briefly described|p36 Fig. 2|Artkinsian|Sakmarian|Geological Province: Canning Basin. See also p39.||||||17-DEC-07
27680|Poole Sandstone|61023|5|Briefly described|p10 Fig. 6|Permian|Permian|Geological Province: Canning Basin.||||||11-APR-08
27680|Poole Sandstone|61551|6|Mentioned|p351 Fig.2. |Artinskian|Sakmarian|||||Overlies Grant Group. Is overlain by Noonkanbah Formation.||
27680|Poole Sandstone|62837|6|Mentioned|Stratigraphic columns|Early Permian|Early Permian|Mentioned only in the context of equivalents. Age: ~290->280Ma. Geological Province:  Fitzroy Trough.||||||09-NOV-06
27680|Poole Sandstone|64186|5|Briefly described|p171, p170 Fig. 1|Artinskian|Artinskian|Includes Nura Nura Member. Underlain by Grant Formation, overlain by Wallal Sandstone. Max thickness: 100m.||||||
27680|Poole Sandstone|64187|5|Briefly described|p320 Fig. 2|Permian|Permian|Underlain by Grant Formation, overlain by Noonkanbah Formation. Sandstone (marine). Geological Province: Canning Basin.||||||03-FEB-10
27680|Poole Sandstone|64580|4|Described|map legend||Early Permian|Quartz sandstone, minor siltstone.||||||17-NOV-08
27680|Poole Sandstone|64630|5|Briefly described|p31 Fig.2|Artinskian|Sakmarian|Province: Northern and Central Canning Basin.  Underlies the Noonkanbah Formation, overlies the Grant Group, includes the Nura Nura Member. Palynology age: P. pseudoreticulata to M. trisina.||||||
27680|Poole Sandstone|64643|4|Described|p8, p3 Fig. 2, p20|Artinskian|Sakmarian|Includes Nura Nura Member. Disconformable on the Grant Group. Conformably overlain by Noonkanbah Formation. Up to 160m thick. Gymnosperm plant rootlets in Mount Piper, Poole Range area correlated with Nura Nura Member although facies are different. ||||||
27680|Poole Sandstone|64971|5|Briefly described|p683, p685 Fig. 2, p689 Fig. 2, p687|Early Permian|Early Permian|Overlies Grant Group, erosional contact. Transgressive shallow marine lithologies.||||||09-FEB-10
27680|Poole Sandstone|64974|5|Briefly described|p143, p148 Fig. 6|Artinskian|Artinskian|Includes Nura Nura Member. Geological Province: Fitzroy Trough.||||||24-JUN-09
27680|Poole Sandstone|64981|5|Briefly described|p669 Fig.3.|Artinskian|Artinskian|||||Overlies Carolyn Formation of Grant Group. Is overlain by Noonkanbah Formation.|Marine to fluvial, fine- to coarse-grained clastic rocks.|
27680|Poole Sandstone|64982|6|Mentioned|p700.|Permian|Permian|||||||
27680|Poole Sandstone|65301|5|Briefly described|p3, p5 Fig. 4|Early Permian|Early Permian|Contains the Nura Nura Member. Overlies units of the Grant Group. Geological province: Canning Basin.||||||
27680|Poole Sandstone|65449|5|Briefly described|p5-6|Cisuralian|Cisuralian|Marginal marine deposits.|||Nura Nura Member.|Unconformably overlies Grant Group. Is overlain by Noonkanbah Formation.||
27680|Poole Sandstone|66127|5|Briefly described|Plates 4, 5, 7.|Permian|Permian|No outcrop in Plate 5 area.||||Overlies Grant Group and is overlain by Noonkanbah Formation.|Well-bedded, fine-grained marine sandstone.|
27680|Poole Sandstone|66949|4|Described|p1, p4 Fig.2, p6, p10-11, p15, p17|Artinskian|Sakmarian|See also p20-23, p28, p31, p34, p46-48,50-54 Appx.2, p56 Appx. 3, p60-65 Appx.4, p66,68-80,82-91 Appx.5; , p119-120 Appx.7; Plates 2-12. Originally mapped as Poole Range Series and lower ferruginous sandstone (Wade, 1937) [In fact Wade used the terms Lower Ferruginous Series, comprising Nura-Nura Beds and their equivalent Upper Beds of Poole Range].Type section detailed. Up to 160 (or 430) m thick; shallow water - fluvial and marine deposits. Diverse fauna listed. Biostratigraphic zonation. Tuckfield and Christmas Creek Members are considered superfluous. Outcrops near S margin of Canning Basin were mapped as Cuncudgerie Sandstone. Reservoir properties discussed. Good to excellent hydrocarbon source potential. Available core and Formation picks detailed. TOC and Rock-Eval data.|||Includes Christmas Creek, Tuckfield and Nura Nura Members.|Disconformably overlies Paterson Formation and Grant Group (unconformably in Fitzroy Trough). Is overlain conformably by Noonkanbah Formation.|Basal carbonate; sandstone and siltstone; thin coaly beds.|
27680|Poole Sandstone|67202|4|Described|p43, p44 Fig.2.10, p67-68, p118-119|Permian|Permian|See also p125-126, p128, p134-135, p141, p248, p253, p281. One of the dominant aquifers in the Canning Basin. Shallow-marine deposits. Conductivity images.||Of Liveringa Group in 1980.||Overlies Paterson Formation. Overlain by the Noonkanbah Formation and unconformably by Callawa Formation.|Interbedded mudstone and fine- to coarse-grained sandstone, thin-bedded, ripple-marked, cross-bedded; minor conglomerate, macrofossils.|22-JAN-20
27680|Poole Sandstone|67354|5|Briefly described|p106, p108 Fig.39.|||Canning Basin.|||Includes Nura Nura Member.|Overlies Clianthus Formation.||
27680|Poole Sandstone|68007|4|Described|p1-2, p4,p6,p9,p12, p14-15, Plates 1, 2|Early Permian|Early Permian|Canning Basin. 97m thick in Patience 2 well. Menzel and Lipski (1986) originally assigned a significantly thicker interval (578?771 m in Patience 1) to the Poole Sandstone. However, the base has been revised upwards in the light of a recent basin-wide reassessment of the Permian stratigraphy (Mory, 2010). Deltaic to shallow marine sediments. Good to excellent reservoir potential. Composite well log. Also appears as Pool Sandstone on p9. Mid-Sakmarian to earliest Artinskian age.||||Overlies Carolyn Formation. Is overlain by Noonkanbah Formation.|White to light grey, moderately to well sorted, fine- to coarse-grained (rarely very coarse-grained) sandstone, with interbeds of light to medium grey silty claystone.|20-FEB-20
27680|Poole Sandstone|68656|6|Mentioned|GEOL_LUT_CSV/500k_geologyp08_lut||Early Permian||||||Quartz sandstone, minor siltstone.|
27680|Poole Sandstone|68902|5|Briefly described|p8, p9 fig 5, p10|Cisuralian|Cisuralian|A thin section of this unit occurs in central Waukarlycarly Embayment. Includes rocks formerly named Cuncudgerie Sandstone (Traves et al., 1956). Distribution is considered largely speculative, as distinguishing this unit from Grant Group or Paterson Formation is not straightforward.|||Includes Nura Nura Member.|Unconformably overlies Grant Group. Is overlain by Noonkanbah Formation.|50m thick, sandstone with brachiopod and bivalve fossil assemblages.|
27680|Poole Sandstone|69029|5|Briefly described|p319,321|Artinskian|Sakmarian|Of Canning Basin. Intraformational shales act as seal to Grant Group reservoirs in the Boundary, Sundown, and West Terrace oilfields on the Lennard Shelf.||||Overlain by Noonkanbah Formation. Underlain by Grant Group.||
27680|Poole Sandstone|69099|5|Briefly described|500k_geologyp08_lut.csv||Early Permian||||||Quartz sandstone, minor siltstone.|04-AUG-15
27680|Poole Sandstone|69165|4|Described|500k_geologyp08_lut.csv|Permian|Permian||||||quartz sandstone, minor siltstone.|
27680|Poole Sandstone|69167|4|Described|geologyp_lut.csv|Cisuralian|Cisuralian||||||Quartz sandstone and minor siltstone.|
27680|Poole Sandstone|69182|5|Briefly described|Ch4 p3, Ch4 p9, Ch4 p15-p16|Cisuralian|Cisuralian|Canning Basin. Potential reservoir for the storage of carbon dioxide that is sealed by the Noonkanbah Formation. See also Ch4 p30-p35, Ch4 p43-p44, Ch4 p45, Ch4 p47, Ch4 p50-p58, Ch4 p63, Ch4 p74-p77, Ch4 p83-p84, Ch4 p87-p88, Ch4 p90. |||Includes the Nura Nura Member.|Overlies the Grant Group. Conformably overlain by the Noonkanbah Formation.|Shallow marine. Fine to medium-grained sandstones with minor coal beds.|
27680|Poole Sandstone|69297|6|Mentioned|p337, p351, p352, p355|Sakmarian|Sakmarian|Broome Platform of the Canning Basin and Canning Basin. Good sealing rock potential. ||Grant Group|Includes the Nura Nura Member|Overlies the Clianthus Formation. Overlain by the Noonkanbah Formation. Unconformably overlain by the Cossigny Member.||
27680|Poole Sandstone|69312|5|Briefly described|p3, p14 fig 13-14, p14 fig 15|Kungurian|Artinskian|Canning Basin. See also  p19, p23 fig 27, p24 fig 28-29, p26 fig 33, p27, p27 fig 34, p28 fig 35. ||||Overlies the Grant Group. Overlain by the Noonkanbah Formation.|Sandstone.|
27680|Poole Sandstone|69547|5|Briefly described|p180,182,190|Artinskian|Sakmarian|Canning Basin.|||Includes Nura Nura Member.|Overlain by Noonkanbah Formation.Underlain by Grant Group.||
27680|Poole Sandstone|69587|5|Briefly described|500k_geologyp08_lut.csv||Early Permian||||||Quartz sandstone, minor siltstone|
27680|Poole Sandstone|69590|4|Described|GEOL_LUT_CSV files|Artinskian|Sakmarian|Of Canning Basin. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|295-287 Ma (biostrat)||||Quartz sandstone and minor siltstone|
27680|Poole Sandstone|69634|5|Briefly described|500k_geologyp08_lut.csv||Early Permian||||||Quartz sandstone, minor siltstone.|
27680|Poole Sandstone|69693|5|Briefly described|p4-6, 9|Sakmarian|Sakmarian|A series of coarsening-upward sequences. Characterised by high amplitude planar seismic reflectors. See also reference to Poole sandstone (p3).||||Unconformably overlies Carolyn Formation (Grant Group). Is overlain by Noonkanbah Formation.|Post-glacial fluvial to marine siliciclastic sediments.|
27680|Poole Sandstone|70065|5|Briefly described|Rowley: Fig.2. Regional: Fig.4; p3, p6|Sakmarian|Sakmarian|Roebuck Basin and offshore Canning Basin.||||Overlies Grant Group. Is overlain by Noonkanbah Formation.|Includes transgressive marine shales.|
27680|Poole Sandstone|70154|5|Briefly described|500k_interpgeop14_lut.csv|Artinskian|Sakmarian||252-273 Ma||||Quartz sandstone and minor siltstone|
27680|Poole Sandstone|70774|3|Fully described|p1-p2, p4-p5, p7-p10,|Early Permian|Early Permian|Canning Basin. Previously described as the 'Poole Range Beds' (Blatchford, 1927). This unit underwent numerous revisions until it was finally designated the Poole Sandstone by Guppy et al., 1951. A type section was defined by Guppy et al., 1958. This unit was correlated with the Cuncudgerie Sandstone before that name was abandoned in favour of making this a basin-wide unit. This formation also previously included the Tuckfield Member and the Christmas Creek Member before being abandoned as unnecessary by Mory (2010). This unit has characteristics suitable for the both storing and trapping CO2. Deposited in an open marine to fluvial environment. Stratigraphic columns are provided in Appendix 2 and lithology is given in detail. Petrographic descriptions are provided in appendix 3. See also p15, p17, p25-p28, p32-p33, p37, p40-p41, p43, p49-p57, p62, p66-p68, p71, p75-p77, p87-p89, p98-p100, Plate 1-Plate 6.|||Includes the Nura Nura Member.|Overlies the Grant Group. Conformably overlain by the Noonkanbah Formation.|Sandstone, siltstones and mudstones.|10-FEB-20
27680|Poole Sandstone|70826|6|Mentioned|p6 tbl 3|Permian|Permian|Canning Basin.||||||
27680|Poole Sandstone|70878|5|Briefly described|p722 Fig.17|Permian|Permian|Fitzroy Trough, NW Canning Basin.||||||
27680|Poole Sandstone|71146|5|Briefly described|p6, p37|Sakmarian|Sakmarian|Canning Basin.||||Disconformably overlies the Grant Group. Overlain by the Noonkanbah Formation.|Sandstone.|
27680|Poole Sandstone|71267|4|Described|GEOL_LUT_CSV files|Artinskian|Sakmarian|Of Canning Basin. Events: Point Moody Extension (300-242 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|292-287 Ma (biostrat-inferred)||||Fossiliferous, locally carbonaceous, ripple marked and cross bedded red-yellow/brown fine and thin-bedded to coarse quartzose sandstone; lenses of white claystone and siltstone and thinly bedded matrix-supported conglomerate; minor coal seams.|
27680|Poole Sandstone|71870|5|Briefly described|p3|Artinskian|Sakmarian|Canning Basin.||||Overlies the Grant Group. Overlain by the Noonkanbah Formation.||
27680|Poole Sandstone|71892|6|Mentioned|p19|||||||||
27680|Poole Sandstone|71894|5|Briefly described|p4|Cisuralian|Cisuralian|Canning Basin.||||Disconformably overlies the Grant Group. Overlain by the Noonkanbah Formation.|Sandstone, carbonate and shale.|
27680|Poole Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Artinskian|Sakmarian|Canning Basin. Max age from biostratigraphy, Min age inferred.|||||Quartz sandstone and minor siltstone.|
27680|Poole Sandstone|72496|5|Briefly described|p218, 220, p223-228|Artinskian|Sakmarian|Canning Basin. Coincides with strong reflection identified in several seismic surveys. Deposited in a shallow water environment.||||Unconformably overlies the Clianthus Formation and the Carolyn Formation (Grant Group). Overlain by the Noonkanbah Formation.||19-MAR-20
27680|Poole Sandstone|72497|3|Fully described|p1, p3, p5, p6 Fig.4, p7, p9, p11.|Artkinskian|Sakmarian|Described as being within the western and eastern St George Ranges, and the Mount Bannerman area. Sediments deposited in shallow marine environment. Shown as occuring in the Anketell, Tabletop, Ryan Shelves, Willara and Kidson Sub-basins, the Jurgurra and Barbwire Terraces and Broome Platform. Also shown as occuring in the Fitzroy Trough, Betty and Balgo Terraces and part of the Lennard Shelf and Margaret Terrace. See also  p12, p15, p18-19, p27, p28.|||Includes Nura Nura Member at base.|Unconformably overlies Grant Group (Millajiddee Member) and conformably underlies Noonkanbah Formation.|Includes light-brown to brown, fine to coarse-grained sandstone.|
27680|Poole Sandstone|72499|4|Described|p1-2, p5, p6, p7, p8, 10-11.|Cisuralian|Cisuralian|Fluvio-deltaic siliciclastic facies intercalated with a local basal carbonate unit. May be shallow marine in part, including tidal flats. Facies recorded on well logs Sundown 1 and Sundown 3/3H (Lennard Shelf) and The Sisters 1 and Scarpia 1 (Fitzroy Trough) and Frome Rocks 2 (Jurgurra Terrace), BMR Mount Anderson 1, Perindi 1. Located in the Willara Sub-basin, Broome Platform and the Fitzoy Trough. This unit is up to 160m thick in places. See also p14, p16, p17-p25, p31, p33-34, p38-41, p43-47, p49, p51, p53, p54 p57-p61, p64-65, p86, p88-89, p93, p95-96, p98-101|||Includes basal Nura Nura Member.|Disconformably overlies Grant Group and conformably (transitionally) underlies Noonkanbah Formation.|Includes microflora and conodont fossils, limestone and very fine sandstone and thin laminae of dark grey organic-rich mudstone. Fine sandstone has local ripple cross-lamination. Lower parts reveal sandstone comprising rounded <10mm pebbles.|
27680|Poole Sandstone|72504|6|Mentioned|Figure 2|||Canning Basin. Overlies Grant Group.||||||
27680|Poole Sandstone|72505|5|Briefly described|p890|Sakmarian|Sakmarian|Canning Basin. Correlates with the Presudo-reticulaspora pseudoreticulata zone.|||Includes the Nura Nura Member.|Unconformably overlies the Grant Group. Overlain by the Noonkanbah Formation.||
27680|Poole Sandstone|73117|5|Briefly described|[See comments].|Sakmarian|Asselian|Canning Basin. Contains part of the Pseudoreticulatispora pseudoreticulata Zone [palynology]. Includes upper sandy facies. The apparently conformable basal contact with the Grant Group is associated with a distinct palynofloral and faunal break including a marked increase in palynomorph diversity. Includes well-dated marine faunas. p: 3, 14-15, 17, 23-25, 28-29, 34, 38-39, 109-117, 120-131, 135-142.|||Nura Nura Member|[Dis]conformably underlain by Grant Group. Overlain by Noonkanbah Formation.|Dominantly sandstone with lesser shale.|
27680|Poole Sandstone|73184|6|Mentioned|p187 Fig.3, p199|Artinskian|Sakmarian|Canning Basin. Post-glacial. Upper Sakmarian to Artinskian age based on palynozones, upper limit to the timing of Permian deglaciation.||||Overlies the Grant Group, underlies the Noonkanbah Formation|Postglacial sandstone.|
27680|Poole Sandstone|73345|6|Mentioned|p230|||Canning Basin. Not present in Barnicarndy 1 well based on palynology results, primarily of Grant Group samples.||||Underlain by Grant Group.||
27680|Poole Sandstone|73445|5|Briefly described|p3, 6, 8, 12, 20, 23-24, 27, 36, 42-43|Permian|Permian|See also p65-118. Canning Basin. Deltaic to marine environment. 160m thick. Age is early Permian. Multi-element spider diagram. Regolith chemistry tabulated.||||Unconformably overlies Grant Group. Is overlain by the Noonkanbah Formation.|Thin-bedded to laminated, well-sorted, fine-grained sandstone and interbedded siltstone; thin carbonaceous beds. Locally cross-bedded; carbonate-rich basal member.|
27680|Poole Sandstone|73574|5|Briefly described|p762|Artinskian|Sakmarian|Northeast Pilbara Craton. Unconformably overlies granite-greenstone bedrock.||||Unconformably overlies Grant Group, unconformably underlies Callawa Formation|Fossiliferous, locally carbonaceous, commonly ripple marked and cross-bedded fine and thin-bedded to coarse quartzose sandstone; lenses of white claystone and siltstone and thinly bedded matrix-supported conglomerate; minor coal seams.|
37649|Pooranoo Metamorphics|61262|2|Defined|p446, p460 App., p445, p447 Fig. 4.|Paleoproterozoic|Paleoproterozoic|Northern Gascoyne Complex; Mangaroon Zone. 2 main units: metamorphosed feldspathic sst, and pelitic gneiss and granofels. Unconformably underlies Edmund Gp. Intruded by Dingo Creek Granite and Durlacher Supersuite plutons. Age: ca1680Ma. Type locality.||||||07-NOV-08
37649|Pooranoo Metamorphics|63246|5|Briefly described|p478 Fig. 1, p480||Paleoproterozoic|Unconformably overlie Morrissey Metamorphics and Moorarie Supersuite. Age: 1680Ma but with 1030-950Ma low-grade schists in central Gascoyne Complex. Metasedimentary rocks - pelitic and semi-pelitic schist and subordinate psammitic schist.||||||07-NOV-08
37649|Pooranoo Metamorphics|63469|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Includes calc-silicate gneiss, migmatitic pelitic gneiss, biot-qtz-musc schists, metamorphosed cobble and pebble conglomerate, sandstone and amphibolite and actinolite-plag schist.||||||07-NOV-08
37649|Pooranoo Metamorphics|63470|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Complex. Gneisses, phyllites, schists; sandstone, pelite, metamorphosed conglomerates; quartzite and schist; amphibolites.||||||07-NOV-08
37649|Pooranoo Metamorphics|63471|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: 1680Ma. Geological Province: Gascoyne Complex. Phyllite; chlorite-muscovite-quartz; locally with magnetite porphyroblasts.Quartzite and muscovite-quartz schist; strongly foliated metamorphosed sandstone, feldspathic sandstone, quartz-lithic sandstone||||||07-NOV-08
37649|Pooranoo Metamorphics|63866|4|Described|p160|Statherian|Statherian|Previously included in the Morrissey Metamorphic Suite. SHRIMP date is interpreted as the maximum depositional age of the sedimentary protoliths and derived from (Sheppard et al., 2005).|1680 +/- 13 Ma (SHRIMP U-Pb)|||Intruded by the Dingo Creek Granite, Pimbyana Granite and the Yangibana Granite.|Pelitic gneiss and metamorphosed feldspathic sandstone with minor amounts of metamorphosed conglomerate, quartz sandstone, amphibolite and calc-silicate rock.|
37649|Pooranoo Metamorphics|63869|4|Described|p1, p4, p5, p10, p12, p16-17, p19|Paleoproterozoic|Paleoproterozoic|See also p22, p23, p25-27, p52, Plate 1. Newly defined; named after Pooranoo Well in SE part of MANGAROON sheet. Previously included in the Morrissey Metamorphic Suite (Williams et al. 1983; Williams, 1986). Deposited after c.1680 Ma; deformed and metamorphosed during the 1680-1620 Ma Mangaroon Orogeny. Maximum depositional age for protoliths of c.1680 Ma.||Unit in Gascoyne Complex.|||Pelitic gneiss and metamorphosed feldspathic sandstone; minor metamorphosed conglomerate, quartz sandstone; very minor amphibolite and calc-silicate rock.|
37649|Pooranoo Metamorphics|64580|4|Described|map legend||Paleoproterozoic|Pelitic schist, gneiss and granofels, and metamorphosed feldspathic sandstone and conglomerate; metamorphosed dolomite.||||||28-OCT-08
37649|Pooranoo Metamorphics|64725|6|Mentioned|p58 Fig.2.|||Capricorn Orogen.||||||
37649|Pooranoo Metamorphics|64728|6|Mentioned|pp106-107.|||Mangaroon Zone, Gascoyne Complex. Medium- to high-grade metasedimentary rocks and minor meta-igneous rocks. Intruded by granites of Durlacher Supersuite.|Maximum depositional age is c.1680 Ma.|||||
37649|Pooranoo Metamorphics|64872|6|Mentioned|p25|||Edmundian Orogeny produced medium-grade fabrics. These are cut by an undeformed granite pluton, the 'Gurun Gutta granite' at ~870 Ma.||||||13-NOV-15
37649|Pooranoo Metamorphics|65152|5|Briefly described|p3.|Paleoproterozoic|Paleoproterozoic|Gascoyne Complex. Siliciclastic sediments including the basal unit,  Mount James Formation. Deposited around 1690-1680 Ma. To the north, they grade upwards into turbiditic sandstone, siltstone and shale; rare amphibolite and calc-silicate rocks.||||||01-MAY-15
37649|Pooranoo Metamorphics|65450|5|Briefly described|p1, p2, p7|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Late Paleopreoterozoic. Pb mineralisation.|c. 1680 Ma.|||Intruded by granite plutons of Durlacher Supersuite at 1680-1660 Ma.|Migmatite; metasedimentary rocks.|
37649|Pooranoo Metamorphics|65453|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Age: c. 1680 Ma (geochronology: Sheppard et al, 2005). Geol. Prov: Gascoyne Province.||||||
37649|Pooranoo Metamorphics|65545|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. c. 1680 Ma. Includes Mount James Subgroup containing the Spring Camp Formation.||||||
37649|Pooranoo Metamorphics|65549|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Gascoyne Province. Includes Mount James Subgroup which includes Spring Camp Formation. Overlies Quartpot Pelite, Camel Hills Metamorphics, underlies Yilgatherra Formation, Edmund Group.||||||
37649|Pooranoo Metamorphics|65830|3|Fully described|p1, p20, p26-33, p35-39; Plates 1,2|Statherian|Statherian|Deformed during 1680-1620 Ma Mangaroon Orogeny. Maximum depositional age from a boulder of psammitic gneiss. |1680 +/- 13 Ma (SHRIMP U-Pb Sheppard et al. 2005)|Of the Gascoyne Complex.||Unconformably overlies Morrissey Metamorphics and the Moorarie Supersuite. Faulted contact with the Mount Augustus Sandstone. Intruded by the Durlacher Supersuite.|Pelitic gneiss and metamorphosed feldspathic sandstone; minor metamorphosed conglomerate, quartz sandstone, amphibolite and calc-silicate rock.|
37649|Pooranoo Metamorphics|66110|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Shown as including the Mount James Subgroup.||||||19-SEP-13
37649|Pooranoo Metamorphics|66299|4|Described|pp3-5, p183, pp215-246.|Paleoproterozoic|Paleoproterozoic|May be source of xenocrysts in Durlacher Supersuite granites. Intruded by granodiorite dated at 1677+/-5 Ma U/Pb SHRIMP. This gives minimum age for Pooranoo Metamorphics. Maximum depositional age uncertain due to uncertainty of stratigraphic position of samples from Mangaroon Zone. Conservative estimate ~1760 Ma.|Min age 1677 +/- 5 Ma. Max age~ 1760 Ma.||Includes Mount James Subgroup.|Intruded extensively by Durlacher Supersuite granites. In isolated localities unconformably overlies Minnie Creek batholith of Moorarie Supersuite. Unconformably overlain by Edmund Group.|Pelitic and psammitic schist, quartz metasandstone, feldspathic metasandstone and metaconglomerate, and phyllite.|17-SEP-14
37649|Pooranoo Metamorphics|66579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|||Shown as consisting only of Mount James Subgroup.||Quartzose schist; quartzose and feldspathic metasandstones; phyllite, slate, metaconglomerate.|
37649|Pooranoo Metamorphics|66887|5|Briefly described|p3 Fig.2, p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Southern Gascoyne Province.|~1760-~1675 Ma estimated from Fig.4.|||||
37649|Pooranoo Metamorphics|66950|5|Briefly described|p9 Fig.8, p10 Fig.9, p12, p13, p15, p17|Statherian|Statherian|Gascoyne Province. Includes rocks reassigned from the now invalid Morrissey Metamorphics, including the type areas from the original "Morrissey Metamorphic Suite" (Williams et al. 1978).|c. 1680 Ma||Includes Mount James Subgroup.|||16-DEC-16
37649|Pooranoo Metamorphics|67247|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|1782 - 1677 Ma.||Includes Mount James Subgroup.|||
37649|Pooranoo Metamorphics|67346|6|Mentioned|p794 Fig.1|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.||||||11-MAY-12
37649|Pooranoo Metamorphics|67371|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|||Includes Mount James Subgroup.|||
37649|Pooranoo Metamorphics|67373|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|||Includes Mount James Subgroup.||Coarse-grained feldspathic metasandstone, quartz-muscovite schist, cobble- and pebble-conglomerate, coarse-grained quartz metasandstone.|
37649|Pooranoo Metamorphics|67843|5|Briefly described|p1, p13.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Sedimentary protoliths were metamorphosed and deformed during the 1030-955 Ma Edmundian Orogeny.|c.1680 Ma.||Includes Mount James Subgroup.|||
37649|Pooranoo Metamorphics|67888|6|Mentioned|p52|||||||||
37649|Pooranoo Metamorphics|68521|5|Briefly described|Map Legend|Statherian|Statherian||c.1780-1680 Ma||Includes Mount James Subgroup.|||
37649|Pooranoo Metamorphics|68522|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. |||Includes Mount James Subgroup.|||
37649|Pooranoo Metamorphics|69003|4|Described|p4, p33-34, p43|Paleoproterozoic|Paleoproterozoic|Gascoyne Province, Capricorn Orogen. Over 6km of siliciclastic sedimentary protoliths underwent high-grade metamorphism and deformation during the 1680-1620 Ma Mangaroon Orogeny, including localised in situ melting..|1760-1680 Ma.||Mount James Subgroup, Coor-de-wandy Formation.|Intruded by Durlacher Supersuite.|Mainly turbiditic sandstones.|
37649|Pooranoo Metamorphics|69028|5|Briefly described|Map Legend|Statherian|Statherian|Gascoyne Province. Includes an unnamed subunit comprising pelitic and psammitic schist, quartz metasandstone, feldspathic metasandstone, and phyllite.|1760-1680 Ma.||Includes the Mount James Subgroup and the Coor-de-wandy Formation.||Includes pelitic and psammitic schist, quartz metasandstone, feldspathic metasandstone and metaconglomerate, and phyllite;  metamorphosed siliciclastic sedimentary rock.|06-MAY-14
37649|Pooranoo Metamorphics|69080|5|Briefly described|p684, p689, p697, p699|Statherian|Statherian|Gascoyne Province. Up to 6 km of turbiditic sediments deposited immediately prior to the 1680-1620 Ma Mangaroon Orogeny.|1760-1680 Ma.||||Pelitic and psammitic schist, quartz metasandstone, feldspathic metasandstone and metaconglomerate, and phyllite.|
37649|Pooranoo Metamorphics|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Age derived from samples of pelitic gneiss and quartz metasandstone (169094.1.pdf, 178746.1.pdf) and suggest maximum ages for sedimentary protolith deposition.|1680 Ma +/- 13 Ma 1698 Ma+/- 9 Ma (SHRIMP)|Gascoyne Complex|Includes Mount James Subgroup||Calc-silicate gneiss, migmatitic pelitic gneiss (diatexite and metatexite migmatite), Pelitic gneiss and granofels; Psammitic schist and gneiss, feldspathic metasandstone interbedded with pelite, quartzite and granule metaconglomerate.|
37649|Pooranoo Metamorphics|69185|4|Described|500k_geologyp08_lut.csv||Paleoproterozoic|Geological Province: Pilbara Craton.|||||Pelitic schist, gneiss and granofels, and metamorphosed feldspathic sandstone and conglomerate; metamorphosed dolomite.|
37649|Pooranoo Metamorphics|69237|5|Briefly described|p1, p4|||Gascoyne Province.|1760-1680 Ma.|||Is intruded by the Gifford Creek Ferrocarbonatite Complex.||
37649|Pooranoo Metamorphics|69387|4|Described|p3, p7-8, p13, p15-23, p27-34, p37|Statherian|Statherian|Mangaroon Zone, Gascoyne Province. Deformation and high-grade metamorphism, including granite magmatism and in situ melting, took place between c.1680-1677 Ma (Mangaroon Orogeny). Underwent medium-grade metamorphism and intrusion during the 1030-955 Ma Edmundian Orogeny. Structural fabric diagrams. SG and magnetic susceptibility values given. Hosts Pb mineralisation. Associated with high-grade W mineralisation at Nardoo Well.|1760-1680 Ma.||Mount James Subgroup.|Is intruded by the Thirty Three Supersuite.|Siliciclastic fluviatile and shallow-marine (turbiditic) sediments: pelitic schists.|
37649|Pooranoo Metamorphics|69546|5|Briefly described|p100-102,105-106|Statherian|Statherian|Geological province: Gascoyne Province. Intruded by Gifford Creek Ferrocarbonite Complex.|1760-1680 Ma|||||
37649|Pooranoo Metamorphics|69583|5|Briefly described|p130, Plate 3.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|1758-1683 Ma.||Mount James Subgroup.||Pelitic and psammitic schist, quartz metasandstone, feldspathic metasandstone and metaconglomerate, and phyllite.|
37649|Pooranoo Metamorphics|69596|5|Briefly described|p5, p9|Statherian|Statherian|Gascoyne Province. Fluvial to shallow-marine deposits; metamorphosed and intruded during the 1680-1620 Ma Mangaroon Orogeny.|c.1740-1680 (precursor deposition).|||Is intruded by Durlacher Supersuite.||
37649|Pooranoo Metamorphics|70019|5|Briefly described|p94|Statherian|Statherian|Geological province: Gascoyne Province, Capricorn Orogen. Comprises Neoarchean to Paleoproterozoic basement rock assemblage of the Gascoyne Province. Package of medium- to high-grade metasedimentary rocks.|1760-1680 Ma|||||
37649|Pooranoo Metamorphics|70127|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Province. Five un-named facies associations are mapped separately.|1741-1682 Ma.||Biddenew Formation.||Feldspathic metasandstone, psammitic schist with interlayered monzogranite, pelitic schist, cobble and pebble metaconglomerate, psammitic gneiss, pelitic gneiss and granofels.|
37649|Pooranoo Metamorphics|70138|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|1741-1682 Ma.|||Is overlain by Yilgatherra Formation (Edmund Group).|Psammitic schist with interlayered leucocratic, or porphyritic biotite, monzogranite; minor pelitic schist; psammitic gneiss, feldspathic metasandstone with interbedded pelite, quartzite and granule metaconglomerate.|10-NOV-15
37649|Pooranoo Metamorphics|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 2_5m_interpgeop15_lut.csv, 100k_geologyl_lut.csv, 100k_interpgeop_lut.csv, 169091.1.pdf, 191994.1.pdf, West Australian Craton|1741-1683 Ma||Includes Mount James Subgroup|Intruded by Thirty Three Supersuite|Migmatitic pelitic gneiss, granofels, psammitic and pelitic schists and gneisses, amphibolite and actinolite-plagioclase schist, cobble and pebble metaconglomerate, metasandstones, calc-silicate gneiss, leucocratic mica monzogranites.|
37649|Pooranoo Metamorphics|70826|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|||||||
37649|Pooranoo Metamorphics|71000|6|Mentioned|p65|Paleoproterozoic|Paleoproterozoic|Southern Gascoyne Province.||||||
37649|Pooranoo Metamorphics|71169|5|Briefly described|p71|Statherian|Statherian|West Australian Craton. |c. 1760-1690 Ma|||||
37649|Pooranoo Metamorphics|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||gneiss, granofels, sandstone, psammite|
37649|Pooranoo Metamorphics|71273|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|1758-1682 Ma.||Biddenew Formation.|||16-FEB-18
37649|Pooranoo Metamorphics|71869|6|Mentioned|p4, p15|||Emplaced during the Mangaroon Orogeny.||||||
37649|Pooranoo Metamorphics|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Capricorn Orogen.|||Includes Mount James Subgroup.||Pelitic and psammitic schist, quartz metasandstone, feldspathic metasandstone and metaconglomerate, and phyllite.|
37649|Pooranoo Metamorphics|72259|6|Mentioned|p3, App. Fig.S5, App. Tb.B|Statherian|Statherian|[Also written as Pooranoo metamorphics, App. Tb.B].|ca. 1760-1680 Ma|||||
37649|Pooranoo Metamorphics|73102|5|Briefly described|p3, p8, p20|Statherian|Statherian|Gascoyne Province.|1758-1682 Ma|||Intruded by Minga Dolerite and Kulkatharra Dolerite.|Pelitic and psammitic schist, quartz metasandstone, feldspathic meta-sandstone and metaconglomerate, and phyllite.|
37649|Pooranoo Metamorphics|73214|5|Briefly described|p974 Fig.1|Palaeoproterozoic|Palaeoproterozoic||||Mount James Subgroup.|||
37649|Pooranoo Metamorphics|73442|5|Briefly described|p3|||Gascoyne Province.|||||Pelitic and psammitic schist, quartz metasandstone, feldspathic metasandstone and metaconglomerate, and phyllite.|
37649|Pooranoo Metamorphics|74493|5|Briefly described|p2, p7|Statherian|Statherian|Gascoyne Province, Mangaroon Zone.|1760-1680 Ma|||Unconformably underlies Edmund Group|Pelitic to arkosic schists, gneisses, and migmatites.|
37649|Pooranoo Metamorphics|74494|5|Briefly described|p1008-1009, p1011-1012, p1014|||||||Intruded by Gifford Creek Carbonatite Complex|Metasedimentary rocks including schists.|
33667|Porphyry Quartz Monzonite|44203|5|Briefly described|Map Legend||Archean|Informal name.||||||07-NOV-08
33667|Porphyry Quartz Monzonite|64775|6|Mentioned|p10-1, Fig. 10.1-10.2|Neoarchean|Neoarchean||2667 +/- 4 Ma.|||||30-MAR-12
33667|Porphyry Quartz Monzonite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Medium- to coarse-grained quartz monzonite; biotite after hornblende; prominent K-feldspar phenocrysts.|07-AUG-15
33667|Porphyry Quartz Monzonite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Medium- to coarse-grained quartz monzonite; biotite after hornblende; prominent K-feldspar phenocrysts.|
33667|Porphyry Quartz Monzonite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||quartz monzonite|
33667|Porphyry Quartz Monzonite|71270|5|Briefly described|1m_geologyp12_lut.csv|||Geological province: Yilgarn Craton, West Australian Craton. |||||Quartz monzonite; mafic granite|
23918|Porpoise Bay Formation|14227|5|Briefly described|Enclos. 2|Oligocene|Eocene|Presented as Porpoise Bay Fm.||||||07-FEB-11
23918|Porpoise Bay Formation|24160|5|Briefly described|p94|Eocene|Eocene|Perth Basin.|||||White chalk, calcarenite, chert.|
23918|Porpoise Bay Formation|41751|2|Defined|p6|middle Eocene||||||||
23918|Porpoise Bay Formation|43700|6|Mentioned|Fig.2,p21||Middle Eocene|||||||
23918|Porpoise Bay Formation|44144|4|Described|p502 Tb.4-21, p518 fig 4-162, p519|Middle Eocene|Middle Eocene|Type Section: Rottnest Island bore; 31o59'55''S 115o32'13''E  285-667m. 382m thick shallow marine deposits.||||Overlies Leederville Formation unconformably and Kings Park Formation disconformably. Is overlain disconformably by Challenger Formation.|Brown calcareous shale and siltstone.|
23918|Porpoise Bay Formation|61155|5|Briefly described|p15|Middle Eocene|Middle Eocene|Age: 47-43Ma. Max. thickness: 350m. Geological Province: Perth Basin.||||||
75580|Port Robinson Basalt|67201|6|Mentioned|p12 Tb.1|||In northwestern Pilbara Craton, West Pilbara Superterrane, Regal Terrane. In informal Cleaverville succession with Dixon Island Formation and Regal Formation.||||||
75580|Port Robinson Basalt|68574|2|Defined|p1, p3-7, p9, p11-14, p39|Mesoarchean|Mesoarchean|New name, after Port Robinson, NW of Roebourne; replaces Dixon Pillow Basalt of Kiyokawa and Taira (1998). NW Pilbara Craton. Crops out on Dixon Island and at Cleaverville Beach. The type area is Dixon Island. Up to 400m thick. Drillcore logs and drillcore tray photographs. Age is based on the conformable relationship to the Dixon Island Formation.|c.3195 Ma.|||Conformably overlies Dixon Island Formation. Is overlain by Cleaverville Formation.|Succession of pillow basalt units and minor massive basalt, with rare dolerite intrusions.|
75580|Port Robinson Basalt|69301|5|Briefly described|p9 Tb.1|||Pilbara Craton. West Pilbara Superterrane. Regal Terrane. Of Cleaverville succession (informal stratigraphic name). |3190 Ma|||Sholl Shear zone above, Regal Thrust below?||
75580|Port Robinson Basalt|70775|5|Briefly described|p12, p19, p28-p29|||Named by Kiyokawa et al., 2012 as the part of the Regal Formation that overlies the Dixon Island Formation.||||Overlies (or is sheared against) the Dixon Island Formation. Equivalent to the Regal Formation.||
29880|Port Smith Sand|64449|2|Defined|p75, p79 Tb. 5, p89-91|Holocene|Holocene|Underlies Eighty Mile Beach Coquina or Cable Beach Sand and Sandfire Calcilutite. Thick: 3m. Age: 3520+/-200 yrs BP, 3680+/-210 yrs BP and 4320+/-220 yrs BP. Consists of grey to brown/tan/buff, bioturbated to laminated sand and shelly sand.||||||07-FEB-11
29880|Port Smith Sand|73213|5|Briefly described|958 Fig.3(a), 959, 965 Fig.13|||||||Is overlain by Eighty Mile Beach Coquina, Cable Beach Sand and Sandfire Calcilutite. Interfingers with Crab Creek Calcilutite Member (Sandfire Calcilutite).|Quartz sand in the low-tidal zone, containing a diverse shelly molluscan biota.|
25410|Portree Granite|22953|6|Mentioned|Fig1p3|||||||||
25410|Portree Granite|23244|6|Mentioned|Fig.2|||||||||
25410|Portree Granite|23789|6|Mentioned|p17 Fig. 4|||Geological Province: Mallina Basin.||||||
25410|Portree Granite|23813|6|Mentioned|p117|||||||||
25410|Portree Granite|24166|5|Briefly described|p3|||||||||
25410|Portree Granite|30766|6|Mentioned|p21|||||||||
25410|Portree Granite|39697|6|Mentioned|p52|||||||||
25410|Portree Granite|43821|5|Briefly described|map legend|Archean|Archean|||||||07-NOV-08
25410|Portree Granite|44150|6|Mentioned|p130-131 Fig.2-130|||||||||
25410|Portree Granite|61267|6|Mentioned|p71|||Pyroxene-hornblende granite.||||||
25410|Portree Granite|63441|2|Defined|p12 tb. 2, p38|Archean|Archean|Of the Portree Suite (Sisters Supersuite). Formerly the Portree Granitic Complex. Age: 2946+/-6Ma U/Pb SHRIMP. Geological province: Pilbara Craton. Rocks are generally massive; medium-grained leucocratic alkali granite in south; coarse-grained alkali granite in north||||Intrudes Mallina Formation.||02-FEB-17
25410|Portree Granite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Portree Suite (Sisters Supersuite). Geological province: Mallina Basin.  Pyroxene-bearing, foliated to massive alkali granite; metamorphosed.||||||07-NOV-08
25410|Portree Granite|64580|4|Described|map legend||Mesoarchean|Of Sisters Supersuite. Pyroxene-bearing, foliated to massive alkali granite; metamorphosed.||||||09-DEC-08
25410|Portree Granite|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Sisters Supersuite.|||Monzogranite; undeformed to foliated; medium-grained, equigranular to weakly porphyritic; weakly metamorphosed|
25410|Portree Granite|69590|4|Described|500k_geologyp08_lut.csv|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; North Pilbara Orogeny.||Unit of Sisters Supersuite.|||Alkali granite, medium-grained, pyroxene-bearing, foliated to massive; metamorphosed|
25410|Portree Granite|70775|5|Briefly described|p29 tbl 5, p66|Mesoarchean|Mesoarchean|Mallina Basin. Also dated at 2946 +/- 6 Ma (Nelson, 1999g).|c. 2950 Ma (Smithies et al 2004a)|Portree Suite|||Massive, medium-grained leucocratic tonalite and granodiorite.|
25410|Portree Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||alkali feldspar granite|
69695|Portree Suite|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Of the Sisters Supersuite.  Alkaline granite. Age: >2.9Ga. Geological Province: Pilbara Craton.  See also p54-55 Fig. 3.||||||07-NOV-08
69695|Portree Suite|63441|4|Described|p12 tb. 2, p38|Archean|Archean|Of the Sisters Supersuite. Contains the Portree Granite with an age of 2946+/-6Ma. Intrudes Mallina Formation. Geological province: Pilbara Craton. Alkaline granite in a series of nested plutons on YULE. See also p33 Fig. 12.||||||07-FEB-11
69695|Portree Suite|63538|6|Mentioned|p6 Fig. 3|Archean|Archean|Geological Province: Pilbara Craton.||||||19-APR-13
69695|Portree Suite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Sisters Supersuite. Contains Portree Granite. Age: c. 2946Ma.||||||07-NOV-08
69695|Portree Suite|66217|5|Briefly described|p42, p43.|Mesoarchean|Mesoarchean|Mallina Basin.|2955-2945 Ma.|Unit in Sisters Supersuite.|||Alkaline granite.|
69695|Portree Suite|67201|4|Described|p7 Fig.4, p22 Fig.13, p23|||West Pilbara Superterrane. In De Grey Superbasin.|2950 Ma|Sisters Supersuite|||Lower crustal, high-temperature alkaline granites.|
69695|Portree Suite|69301|5|Briefly described|p5 Fig.3|||Pilbara Craton. West Pilbara Superterrane.|||||Granitic rocks.|
69695|Portree Suite|69590|4|Described|250k_interpgeop_lut.csv|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; North Pilbara Orogeny.|2946 MA (isotopic)|Unit of Sisters Supersuite.|||Granitic rock; metamorphosed|
69695|Portree Suite|70022|6|Mentioned|p115|||West Pilbara Superterrane.||||||
69695|Portree Suite|70775|5|Briefly described|iii, p41, p64-p66|||Geochronology indicates that this suite is coeval with the Indee Suite.|c. 2946 Ma||Includes the Portree Granite.|||
69695|Portree Suite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||2946+/-6 Ma|Sisters Supersuite|||Granitic rock; metamorphosed.|
69695|Portree Suite|72668|5|Briefly described|p4, p15, p17, p22|||West Pilbara Superterrane.|c. 2946 Ma|Sisters Supersuite|||Alkaline granites.|
32213|Potkoorok Member|61266|4|Described|p57|Archean|Archean|Of the Euro Basalt. Thickness: ~2800m. Interlayered pillow basalts and various cherts. Paraconformably to unconformably underlies the Sulphur Springs Group. Geological Province: Pilbara Craton.||||||07-NOV-08
33649|Pottoyu Granite Suite|24301|6|Mentioned|p37 Appendix 1|||||||||
33649|Pottoyu Granite Suite|50286|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Musgrave Block.  Age: ~1190 - 1140Ma.||||||31-MAY-04
33649|Pottoyu Granite Suite|50321|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Musgrave Block. Age: ~1190-1140Ma. Includes Amputjuta Dacite and Ilyaralana Granite.||||||06-MAY-13
33649|Pottoyu Granite Suite|60572|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the Mulyati Granite and undivided Pottoyu Granite Suite rocks. Age: ~1190-1140Ma.||||||06-MAY-13
33649|Pottoyu Granite Suite|60683|1|Redefined|p56-57 Appendix, p16-17|Mesoproterozoic|Mesoproterozoic|Formerly the Pottoyu Granite Complex of Forman (1966a, 1972) and parts previously mapped as Olia Gneiss. Coarsely porphyritic biotite granite, typically with rapakivi texture. Age: 1192+/- and 1144+/-12Ma (SHRIMP U-Pb zircon). See also p11 Tb. 1, p42-43.||||||23-DEC-09
33649|Pottoyu Granite Suite|61154|6|Mentioned|p44 Appendix|Mesoproterozoic|Mesoproterozoic|Possibly an informal name? - see also Pottoyu Suite. Of the Pitjantjatjara Supersuite.||||||23-NOV-06
33649|Pottoyu Granite Suite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the Mulyati and Ilyaralona Granites, and Ampitjuta Dacite. Age: ~1190-1140Ma. Geological Province: Musgrave Block.||||||06-MAY-13
33649|Pottoyu Granite Suite|63866|5|Briefly described|p202, p206|||Musgrave Province. See also Pottoyu Suite [unclear which name takes precedence].||Pitjantjatjara Supersuite||||
33649|Pottoyu Granite Suite|65256|4|Described|piii, p5-9, p7, p38, p31|Stenian|Mesoproterozoic|Includes Amputjuta Dacite, Ilyaralona Granite. Coarsely porphyritic biotite granite, typically with rapakivi texture; less abundant equigranular granite and aplite. Unconformably underlies Karukali Quartzite or Dean Quarzite or Kulail Sandstone. SHRIMP U-Pb ages of 1192+/-13 Ma and 1144+/-12 Ma; Rb-Sr whole rock ages of 1150 and 1190 Ma. Intruded by mafic dykes interpreted to belong to Alcurra dolerite. Suggested source of sediment for Karukali Quartzite. Given as Pottoyu Suite and Pottoyu Granite on piii.||||||
33649|Pottoyu Granite Suite|69091|5|Briefly described|p85, p137-139 Figs.6.4-6.6|||Name shortened to Pottoyu Suite in legend on p137-139 Figs.6.4-6.6.||Pitjantjatjara Supersuite|||Amphibolite facies metagranites.|
33649|Pottoyu Granite Suite|70793|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma); Musgrave Orogeny (1220-1150 Ma). See 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 500k_interpgeop_lut.csv.|1192+\-13 Ma; 1148+\-12 Ma|Unit of Pitjantjatjara Supersuite.|||Fine- to coarse-grained, foliated, biotite metagranite|
33649|Pottoyu Granite Suite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
33649|Pottoyu Granite Suite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma); Musgrave Orogeny (1220-1150 Ma). See 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|1192+\-13 Ma; 1148+\-12 Ma|Unit of Pitjantjatjara Suite.|Includes Amputjuta Dacite.||Fine- to coarse-grained, foliated, biotite metagranite|
33649|Pottoyu Granite Suite|71592|5|Briefly described|Appendix A.|||Musgrave Province. Both crystallisation ages: U-Pb zircon SHRIMP.|1192+/-13 Ma and 1144+/-12 Ma.||||Granite.|
33649|Pottoyu Granite Suite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Musgrave Province, Paterson Orogen.|Max age 1192+/-13 Ma, Min 1148+/-12 Ma.|Pitjantjatjara Supersuite|||Fine- to coarse-grained, foliated, biotite metagranite.|
33203|Powdar Monzogranite|24166|6|Mentioned|p18|Archean|Archean|Age: 2935-2930Ma (Nelson, 1999)||||||07-NOV-08
33203|Powdar Monzogranite|24533|5|Briefly described|p7, p4 Table 1|Archean|Archean|Of the Yule Granitoid Complex. Includes four distinct mineralogical and textural varieties of rock but only a porphyritic monzogranite and seriate-textured monzogranite are exposed on HOOLEY. Age: 2935 +/- 3Ma.||||||07-NOV-08
33203|Powdar Monzogranite|24534|5|Briefly described|Map legend|Archean|Archean|Of the Yule Granitoid Complex.  Age: 2935Ma.||||||07-NOV-08
33203|Powdar Monzogranite|50370|5|Briefly described|Map Legend|Archean|Archean|Of Yule Granitoid Complex. Geological Province: Pilbara Craton. Age: c. 2935 Ma||||||07-NOV-08
33203|Powdar Monzogranite|63372|4|Described|Map Legend|Archean|Archean|Of the Yule Granitoid Complex. Geological Province: East Pilbara Granite-Greenstone Terrane.  Age: 2935Ma. Biotite-bearing monzogranite and syenogranite; weakly foliated to massive; metamorphosed.||||||07-NOV-08
33203|Powdar Monzogranite|63441|5|Briefly described|p11 Tb. 2|Archean|Archean|Of Sisters Supersuite. Geological province: Pilbara Craton.||||||07-FEB-11
33203|Powdar Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, syenogranite|
33203|Powdar Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||2935+/-3 Ma.|Sisters Supersuite|||Leucocratic monzogranite; locally coarsely porphyritic; metamorphosed.|
79517|Powder Gabbro|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2696 Ma (inferred).|Leviathan Suite|||Gabbro; metamorphosed. Leucogabbro; coarse grained with granophyric texture; metamorphosed.|
79517|Powder Gabbro|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2696 Ma (inferred)|Unit of Leviathan Suite.|||Gabbro; common hornblende-plagioclase-quartz-titanite assemblage; metamorphosed; Leucogabbro; coarse-grained with granophyric texture; metamorphosed.|
73848|Power Hill Formation|24391|4|Described|p8-4 Fig.2|Archean|Archean|Of Point Samson Group. Felsic volcanics, black-white chert, felsic tuff, ferruginous chert and banded iron formation. Geological Province: Pilbara Block.||||||07-NOV-08
70614|Power House Cherts|62406|6|Mentioned|p55 Fig. 3|||Possibly informally named rocks associated with a power complex in the Golden Mile area?||||||
22692|Poynton Formation|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Rudall Complex, Paterson Orogen.||||||
22692|Poynton Formation|23602|4|Described|p11|||See also page 6 Table 1. Of Rudall Complex. Underlying unit Butler Creek Formation. Max. thickness: >1000 m.||||||
22692|Poynton Formation|23760|4|Described|p16|Proterozoic|Proterozoic|Geological Province: Talbot Terrane.||||||
22692|Poynton Formation|43848|5|Briefly described|Map Legend||Proterozoic|||||||
22692|Poynton Formation|50436|6|Mentioned|p2.1|||Overlies: Yandagooge Formation.||||||
22692|Poynton Formation|64580|6|Mentioned|map legend|||Quartzite, psammitic paragneiss, banded paragneiss, and pelitic schist.||||||15-DEC-08
22692|Poynton Formation|64943|4|Described|p4-6, p8-9,10,11,13,19,28,35,37,39|Paleoproterozoic|Paleoproterozoic|Talbot Terrane, Rudall Complex. Max thickness 1000 m; metamorphosed quartzite, greywacke, and minor pelite and banded BIF. Overlies/ is faulted against Butler Creek Formation; unconformably overlain by Coolbro Sandstone. Type locality given.||||||
22692|Poynton Formation|65454|6|Mentioned|p4, p30 Fig.A1b|Statherian|Statherian|Of Fingoon Package, Talbot Terrane. Age uncertain but experienced Yapungku Orogeny ~1800-1760 Ma or ~1680 Ma, and an earlier event?||||||21-APR-16
22692|Poynton Formation|67202|5|Briefly described|p56|||Talbot Terrane, Rudall Complex. c.1km thick.|||||Quartzite, greywacke, quartz-muscovite schist, minor pelitic schist and BIF.|
22692|Poynton Formation|68981|5|Briefly described|p3|||Eastern Talbot Terrane, Rudall Province.||||Overlies Yandagooge Formation.|Quartzite and quartz-feldspar-mica gneiss.|
22692|Poynton Formation|71169|5|Briefly described|p3-p4, p6-p7, p18, p60|||||||Structurally overlies the Butler Creek Formation.||
22692|Poynton Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||pelite, psammite, felsic schist, quartzite|
22692|Poynton Formation|71795|6|Mentioned|p35 fig 4|||Rudall Province.||||||
22692|Poynton Formation|73168|6|Mentioned|p741 Fig.2|Mesoproterozoic|Paleoproterozoic|Rudall Province.||||||
80100|Prairie Downs Dyke Suite|70826|6|Mentioned|p14 tbl 5|Neoarchean|Neoarchean|South Pilbara Craton.|2745 Ma|||||
26854|Premier Coal Measures|14227|5|Briefly described|Enclos. 2|Permian|Permian|Underlies Muja Coal Measures; overlies Allanson Sandstone. Presented as Premier C. M.||||||07-FEB-11
26854|Premier Coal Measures|22820|6|Mentioned|p21|||Of the Collie Group. Geological province: Collie Basin. Correlate with Redgate C. M.||||||11-JAN-10
26854|Premier Coal Measures|23174|5|Briefly described|Fig5p8|||||||||
26854|Premier Coal Measures|42711|2|Defined|p5 Fig. 4, p25, Plates 2, 4, 5|Early Permian|Early Permian|Of Collie Group. Supersedes Premier Member; also known as "Chicken Creek Member", Collie Burn Member. Thickness: 320m. Geol.prov: Collie Basin. Comprises a multitude of thick and thin coal seams + intercalating sandstone/siltstone. Lith.details given.||||||11-AUG-08
26854|Premier Coal Measures|43442|6|Mentioned|p50|||||||||
26854|Premier Coal Measures|64580|6|Mentioned|map legend|||Of Collie Group.||||||15-DEC-08
26854|Premier Coal Measures|64630|5|Briefly described|p31 Fig.2|Roadian|Kungurian|Province: Collie Subbasin. Overlies the Allandale Sandstone, underlies the Muja Coal Measures. Palynology age: P. sinuosus to D. granulata. Top correlates with the top of the Redgate Coal Measures.||||||24-NOV-09
26854|Premier Coal Measures|70097|5|Briefly described|p19 Fig.3|Roadian|Kungurian|Southern Perth Basin. Collie Sub-basin.||Collie Group||Overlies Allanson Sandstone. Is overlain by Muja Coal Measures.|Includes coal.|12-SEP-17
26854|Premier Coal Measures|70774|5|Briefly described|p5 fig 3|Ufimian|Kungurian|Collie Basin.||||Overlies the Allandale Sandstone. Unconformably? Overlain by the Muja Coal Measures.||
26854|Premier Coal Measures|72034|5|Briefly described|500k_interpgeop16_lut|Kungurian|Artinskian|Perth Basin.  Age from biostratigraphy.||Collie Group.|||Interbedded poorly sorted feldspathic sandstone, carbonaceous shale, coal; pebble conglomerate.|
78516|Prendergast Sandstone|68107|4|Described|p608 Fig.4, p613, p616.|Neoarchean|Neoarchean|Of Standing (2008). Laverton Greenstone Belt, Burtville Terrane. Contains a detrital zircon population dated at 2775 +/- 4, and a single grain dated at 2748 +/- 9 Ma (Barley et al. 2006).|rhyolitic breccia 2758 +/- 6 Ma Barley et al 2006||||Comprises arkosic sandstone and felsic volcaniclastic rocks.|15-NOV-13
78516|Prendergast Sandstone|71168|6|Mentioned|p10|Neoarchean|Neoarchean|Burtville Terrane, Yilgarn Craton.|2758 +/- 6 Ma|||||
78516|Prendergast Sandstone|73596|6|Mentioned|p1170|Neoarchean|Neoarchean|Laverton Greenstone Belt, Burtville Terrane.|2751 +/- 6 Ma (MDA).|||Overlies Burtville Sandstone. Is overlain by Merolia Rhyolite.||
36150|Prenti Dolerite|24535|4|Described|p2, 4, 10-11, 15-16|Stenian|Stenian|Age: c. 1070 Ma (shown as 1050 Ma from Compston, 1974 in Fig 15). Plagioclase and augite. Geological Province: Earaheedy Basin. Dating and palaeomagnetism described. Intrudes Earaheedy Group, Glenayle Dolerite..||||||26-NOV-13
36150|Prenti Dolerite|63866|6|Mentioned|p178|||||||||
36150|Prenti Dolerite|64572|6|Mentioned|p810 Fig. 10|Neoproterozoic|Neoproterozoic|Age: ca. 1050Ma (K-Ar).||||||22-DEC-08
36150|Prenti Dolerite|64580|4|Described|map legend||Mesoproterozoic|Of Warakurna Supersuite. Dolerite sill, dyke, and plug; fine- to coarse-grained dolerite.||||||15-DEC-08
36150|Prenti Dolerite|64655|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Aphanitic dolerite, plagioclase phyric.||||||
36150|Prenti Dolerite|64772|4|Described|p15, Plate 1  legend|Mesoproterozoic|Mesoproterozoic|Part of the Warakurna Large Igneous Province. Age: c.1070Ma. Intrudes the Glenayle Dolerite. Aphanitic to very fine-grained dolerite sills and dykes. Not determined whether the Glenayle Dolerite and Prenti Dolerite are comagmatic or represent separate magmatic events.||||Intrudes Glenayle Dolerite.||25-NOV-13
36150|Prenti Dolerite|65899|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age shown as c.1070 Ma. Unit in Warakurna Supersuite. Shown as combined Glenayle and Prenti Dolerites, with one description: Dolerite sill, dyke and plug; fine- to coarse-grained dolerite.||||||
36150|Prenti Dolerite|66256|6|Mentioned|p17 Fig.13|||Earaheedy Basin.||||||
36150|Prenti Dolerite|66427|6|Mentioned|p42, p44-45   |||Part of the Warakurna Large Igneous Province.|1076 Ma.|||||
36150|Prenti Dolerite|67375|6|Mentioned|p14 Fig.9. |||Part of the Warakurna Large Igneous Province.||||||
36150|Prenti Dolerite|67553|6|Mentioned|p15|||Of Earaheedy Basin, part of the Warakurna Large Igneous Province.||||||
36150|Prenti Dolerite|69003|6|Mentioned|p50 Fig.59|||||||||
36150|Prenti Dolerite|69152|5|Briefly described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Grouped as Glenayle and Prenti Dolerites||Warakurna Supersuite|||Dolerite sill, dyke, and plug; fine- to coarse-grained dolerite.|07-AUG-15
36150|Prenti Dolerite|70153|5|Briefly described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|Shown with Glenayle Dolerite as its parent. [If so, this needs to be called the Prenti Dolerite Member]. See also 100k_geologyp14_lut.csv and 500k_interpgeop14_lut.csv.|1066 Ma (inferred).|Warakurna Supersuite.|||Dolerite sill; fine- to medium-grained dolerite.|
36150|Prenti Dolerite|70826|6|Mentioned|p10|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||Warakurna Supersuite.||||20-MAY-20
36150|Prenti Dolerite|71210|6|Mentioned|p5, p11|||||Warakurna Supersuite||||
36150|Prenti Dolerite|71270|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Of Warakurna Large igneous Province. Events: Alice Springs Orogeny (450 - 295 Ma); Petermann Orogeny (580 - 520 Ma); Paterson Orogeny (635 - 540 Ma); Warakurna Supersuite Magmatic Event (1084 - 1040 Ma); Giles Event (1085 - 1040 Ma). See 500k_interpgeop16_lut.csv, 100k_geologyp14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv.|1066 Ma|Unit of Warakurna Supersuite.|||Dolerite sill; fine- to medium-grained dolerite|
36150|Prenti Dolerite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|||Glenayle Dolerite|||Dolerite sill; fine- to medium-grained dolerite.|
73569|Preston Beach Coquina|63454|2|Defined|p71 Tb. 3, p77|Holocene|Holocene|Conformably overlain by Safety Bay Sand; erosional contact with both Becher Sand and Leschenault Formation below. Max. thickness: 7m. White, cream, yellowish and tan shell beds, shell grit, shelly sand, and coarse to medium sand.||||||
80576|Prince Regent Dolerite|71811|5|Briefly described|Map legend.|Permian|Carboniferous|Typically NW-trending dykes.|||||Dolerite dykes.|
69036|Princess Creek Group|44231|5|Briefly described|Section only|Ordovician|Ordovician|Dolomite, limestone, sandstone and shale; marine deposits.||||||
36893|Princess Ranges Member|23529|5|Briefly described|p10|Paleoproterozoic|Paleoproterozoic|Formerly Princess Ranges Quartzite. Parent: Chiall Formation. Max. thickness: ~500m. Geological Province: Earaheedy Basin.||||||07-NOV-08
36893|Princess Ranges Member|23589|5|Briefly described|p28|||Previously Princess Ranges Quartzite. Of Chiall Formation. Earaheedy Basin.||||||
36893|Princess Ranges Member|24017|5|Briefly described|p12 Fig. 5|||Formerly Princess Ranges Quartzite.  Of the Chiall Formation.||||||07-AUG-08
36893|Princess Ranges Member|24578|5|Briefly described|p778 Fig.3|Paleoproterozoic|Paleoproterozoic|Of the Chiall Formation. Geological Province: Earaheedy Basin.||||||07-NOV-08
36893|Princess Ranges Member|50188|5|Briefly described|p4 Fig. 2, p6-7|Paleoproterozoic|Paleoproterozoic|Of the Chiall Formation. Characterised by presence of quartz arenite.||||||07-NOV-08
36893|Princess Ranges Member|50195|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Chiall Formation. Geological Province: Earaheedy Basin.||||||07-NOV-08
36893|Princess Ranges Member|50222|5|Briefly described|p320 Fig. 3|Paleoproterozoic|Paleoproterozoic|Formerly the Princess Ranges Quartzite.  Now a member of the Chiall Formation (Miningarra Subgroup, Earaheedy Group). Glauconite.  Geological Province: Earaheedy Basin.||||||07-NOV-08
36893|Princess Ranges Member|50223|5|Briefly described|p345 Fig. 2, p346|Paleoproterozoic|Paleoproterozoic|Of the Chiall Formation (Miningarra Subgroup, Earaheedy Group). Quartz arenite, interbedded with siltstone. Conformably overlain by Wongawol Formation. Detrital Zr ages: 2.9-1.9Ga. Max. thickness: 32m. Geological Province: Earaheedy Basin. See also p355.||||||01-MAR-10
36893|Princess Ranges Member|50378|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Chiall Formation (Miningarra Subgroup). Geological Province: Earaheedy Basin. Fine- to medium-grained sandstone, generally texturally mature, locally pebbly and glauconitic; subordinate siltstone, shale and mudstone.||||||07-NOV-08
36893|Princess Ranges Member|64284|5|Briefly described|p60 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of Chiall Formation (Minningarra Subgroup). Formerly Princess Ranges Quartzite and small part of Wandiwarra Member. Geological Province: Earaheedy Basin||||||07-FEB-11
36893|Princess Ranges Member|64772|5|Briefly described|p12, p10 Fig. 5, p26 Fig. 13|Paleoproterozoic|Paleoproterozoic|Supersedes "Princess Ranges Quartzite". Of Chiall Fm. See also p32 Fig.20, p44 Fig.30, p75 App.4 Tb.4.3, p78 App.4 Tb.4.4|||||Sandstone.|25-NOV-13
36893|Princess Ranges Member|65472|5|Briefly described|p3 Fig.2|||Age: from Fig.2, after Pirajno et al. Earaheedy Basin.|1.85 Ma detrital zircon U-Pb SHRIMP youngest age|Chiall Formation||||
36893|Princess Ranges Member|65692|6|Mentioned|p55|||||Chiall Formation.||||
36893|Princess Ranges Member|66427|5|Briefly described|p44 Tb.2, p46-48, p63, p65-70      |||Here replaces Princess Ranges Quartzite; see references to that unit at p46 Fig.4, p63. Recognised as part of a single depositional episode. SHRIMP U-Pb detrital zircon age.|1876 +/- 19 Ma (Halilovic et al., 2004).|Unit in Chiall Formation.|||Generally comprises shale, siltstone, mudstone units interbedded with very fine-grained sandstone, and siltstone-dominated units and mature quartz arenite.|
36893|Princess Ranges Member|69003|5|Briefly described|p14 Fig.18|||Earaheedy Basin.||Chiall Formation.||Is overlain ?conformably by Wongawol Formation.||
36893|Princess Ranges Member|69152|4|Described|1m_geologyp08_lut.csv|Orosirian|Orosirian|||Chiall Formation|||Clean white quartz sandstone, minor clayey sandstone and siltstone.|07-AUG-15
36893|Princess Ranges Member|69313|5|Briefly described|p25 Fig.4.3|||||Chiall Formation||Overlain by the Wongawol Formation. Overlies the Wandiwarra Member.|Sandstones.|
36893|Princess Ranges Member|69596|6|Mentioned|p10|||Earaheedy Basin.||Chiall Formation.||||
36893|Princess Ranges Member|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone|
36893|Princess Ranges Member|71270|5|Briefly described|1m_geologyp12_lut.csv|||||Unit of Chiall Formation.|||Fine- to medium-grained sandstone, generally texturally mature, locally pebbly and glauconitic; subordinate siltstone, shale and mudstone.|
38728|Princess Royal Member|24397|5|Briefly described|p243-244, p242|||Replaces Princess Royal Spongolite.  Geological Province: Eucla Basin.||||||
38728|Princess Royal Member|64340|5|Briefly described|p26 Tb. 5|Late Eocene|Late Eocene|Of Pallinup Formation (Eundynie Group).||||||28-JUL-09
38728|Princess Royal Member|65194|5|Briefly described|p138 Fig.4.38|Late Eocene|Middle Eocene|Shown as unit in Pallinup Formation (Clarke et al 2003).||||||
38728|Princess Royal Member|65260|6|Mentioned|p26, p27 Fig.20|Late Eocene|Late Eocene|Spongolitic. Interfingers with the Hampton Sandstone in the Lefroy Palaeochannel. Most likely correlates with Eundynie Group. Proposed by Clarke (2003) as part of Pallinup Formation.||||||
38728|Princess Royal Member|69152|4|Described|1m_geologyp08_lut.csv|Eocene|Eocene|||Pallinup Formation|||Spongolite, sandstone, siltstone, claystone, locally silicified.|07-AUG-15
38728|Princess Royal Member|69598|5|Briefly described|p2, p9, p11 Tb.1, p29 Tb.4|Late Eocene|Late Eocene|Eucla Basin. Potential carbon dioxide storage reservoir. Contains potential sealing lithologies. Also referred to as the Princess Royal Spongolite on p9.  ||Pallinup Formation||||
38728|Princess Royal Member|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||spongolite, sanstone, siltstone, claystone|
38728|Princess Royal Member|71270|5|Briefly described|1m_geologyp12_lut.csv|||Of Eucla Basin.||Unit of Pallinup Formation.|||Spongolite, sandstone, siltstone, claystone, locally silicified|
31874|Pungkuli Formation|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Throssell Group, Yeneena Basin.||||||
31874|Pungkuli Formation|23602|5|Briefly described|p15|||Of Throssell Group. Overlying unit Gunanya Sandstone.||||||
31874|Pungkuli Formation|23742|4|Described|p6||Mesoproterozoic|Underlying unit Taliwanya Formation. Max. thickness: 900 m.||||||
31874|Pungkuli Formation|23760|4|Described|p24|Proterozoic|Proterozoic|Of Throssell Group. Geological Province: Yeneena Basin. Max. thickness: 900 m.||||||
31874|Pungkuli Formation|24594|5|Briefly described|p601|Neoproterozoic|Mesoproterozoic|Of the Throssell Group.  Geological Province: Yeneena Basin (Paterson Orogen).||||||09-JUL-13
31874|Pungkuli Formation|43848|5|Briefly described|Map Legend||Proterozoic|Of Throssell Group, Yeneena Supergroup.||||||
31874|Pungkuli Formation|43849|5|Briefly described|Map Legend||Proterozoic|Of Throssell Group.||||||
31874|Pungkuli Formation|62453|3|Fully described|p68|Cryogenian|Cryogenian|Of the Throssell Range Group. Paterson Orogen. Overlies: Taliwanya Formation. Thicknes: 900m. Shale, siltstone, sandstone, carbonate and chert. ||||||
31874|Pungkuli Formation|64580|4|Described|map legend|Neoproterozoic|Mesoproterozoic|Reddish brown to grey shale, locally carbonaceous; minor sandstone, dolomite, and sulfidic shale and sandstone; Fine- to medium-grained sandstone; well bedded; minor siltstone and shale.||||||15-DEC-08
31874|Pungkuli Formation|65403|4|Described|pp13-14, p20, p25.|||New name. Named after local name for McKay Range. c.900 m thick. Greenschist facies metamorphosed; folds and cleavage from the Miles Orogeny have been refolded by later events. May be prospective for base-metal deposits.||Unit in Throssell Group.||Conformably overlies Taliwanya Formation. Is overlain disconformably by Gunanya Sandstone of the Tarcunyah Group.|Interbedded, laminated, slightly micaceous, grey to dark-brown-black shale; locally carbonaceous shale and siltstone; thin units of sulfidic shale and sandstone; minor carbonate rocks and chert.|
31874|Pungkuli Formation|65454|5|Briefly described|p7-8, p10-11|Cryogenian|Cryogenian|Yeneena Basin. Of Throssell Range Group. Locally derived sandstones and shales.||||||
31874|Pungkuli Formation|67182|6|Mentioned|p677 Fig.2|Neoproterozoic|Neoproterozoic|||||||
31874|Pungkuli Formation|67202|4|Described|p58, p65, p138, p157, p233, p235|Neoproterozoic|Mesoproterozoic|See also p237-238, p241, p243, p247. 900m thick. Conductivity imaged and discussed. A potential reductant for uranium mineralisation.||Throssell Range Group.||Conformably overlies Taliwanya Formation. Is overlain by Coolbro Sandstone. May correlate with Broadhurst Formation.|Reddish-brown to grey-black shale, minor sandstone, carbonate and pyritic shale.|
31874|Pungkuli Formation|67430|6|Mentioned|p22|||Paterson Province.||||||
31874|Pungkuli Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||shale, crystalline dolostone/dolomite, sulphide-rich rock|
33811|Puntitjata Rhyolite|50286|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. Age: ~1075Ma.||||||03-AUG-09
33811|Puntitjata Rhyolite|50321|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: ~1075Ma. Of the Tjauwata Group.||||||28-MAY-04
33811|Puntitjata Rhyolite|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. Porphyritic rhyolite. Geological Province: Musgrave Block.||||||03-AUG-09
33811|Puntitjata Rhyolite|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Rhyolite. Geological Province: Musgrave Block. Of Tjauwata Group.||||||14-JAN-05
33811|Puntitjata Rhyolite|61154|5|Briefly described|p16, p18 Fig. 10|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. Porphyritic rhyolite; tuff and epiclastic sediments. Overlies Mount Harris Basalt; transitionally overlain by Bloods Range Formation. Age: 1075+/-2Ma. Geological Province: Musgrave Block. See also p5Tb. 1, p44 Appendix.||||||03-AUG-09
33811|Puntitjata Rhyolite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group.  Porphyritic rhyolite.||||||19-OCT-05
33811|Puntitjata Rhyolite|62989|5|Briefly described|p39|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. Age: 1075+/-2.5Ma. extrusive equivalent of the intrusive Hull Granite Suite. Correlated with Smoke Hill Volcanics of the Tollu Group in WA.||||||25-JAN-07
33811|Puntitjata Rhyolite|63866|4|Described|p203|Stenian|Stenian|Mulga Park Domain, Musgrave Province. Numeric age is a Pb-Pb Kober zircon age.|1075 +/- 3 Ma (Close et al., 2003)|Tjauwata Group||Overlies the Mount Harris Basalt.||
33811|Puntitjata Rhyolite|64745|5|Briefly described|p376|Stenian|Stenian|Paper implies of Tollu Group. Age: ca. 1.075Ga.||||||
33811|Puntitjata Rhyolite|65135|5|Briefly described|p16|Stenian|Stenian|Of Tjauwata Group. Dated at 1075 +/- 3 Ma.||||||
33811|Puntitjata Rhyolite|65256|2|Defined|p6 Tb.1, p11-12, p14 Fig 10, p37, p39|Stenian|Stenian|New name: within the upper stratigraphy of the Tjauwata Group. Finely porphyritic rhyolite, tuff, minor volcaniclastics. A-type. Overlies or is laterally equivalent to Mount Harris Basalt; underlies Bloods Range Formation gradationally, or Kulail Sandstone/Dean Quartzite. Pb-Pb evaporation on zircon age 1075+/-2.5 Ma; coeval and correlated with Smoke Hill Felsic Volcanics (Tollu Group).||||||
33811|Puntitjata Rhyolite|65833|5|Briefly described|p16|Stenian|Stenian|Of Tjauwata Group. 1075 +/- 3 Ma: a c.30 m.y. gap between this unit and the Wankari Volcanics, also of Tjauwata Group. Possible age equivalent of Skirmish Hill Volcanics.||||||
33811|Puntitjata Rhyolite|65906|5|Briefly described|p19, p22|Mesoproterozoic|Mesoproterozoic|Unit in Tjauwata Group and is a correlative of the Smoke Hill Volcanics. Age 1075 +/- 3 Ma (Edgoose et al., 2004).||||||
33811|Puntitjata Rhyolite|67128|5|Briefly described|p3, p12, p18, p27, p30|||Western Bloods Range. Age equivalent of Skirmish Hill Volcanics.|1075 +/- 2 Ma (Close et al., 2003).|Tjauwata Group.||Extrusive equivalent of Rowley Granophyre.||
33811|Puntitjata Rhyolite|67375|5|Briefly described|p217.|Mesoproterozoic|Mesoproterozoic|May post-datre many Giles Suite intrusions, negating a tentative correlation with the Kunmarnara Group.|c.1075 Ma.|Unit in Tjauwata Group.||||
33811|Puntitjata Rhyolite|69436|4|Described|p21:4, 13-14|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Has been broadly correlated with Smoke Hill Volcanics based on their implied stratigraphic positions and geochronological ages. Also appears as Puntijata Rhyolite in 21:14. Kober Pb-Pb zircon age.|1075 +/- 3 Ma (Close et al., 2003).|Tjauwata Group.||Overlies, or is laterally equivalent to, Mount Harris Basalt. Is overlain transitionally by Bloods Range Formation. Correlated with Wankari and Smoke Hill Volcanics.|A succession of rhyolite flows, tuff and epiclastic sedimentary rocks. A-type.|12-JUL-16
33811|Puntitjata Rhyolite|70018|4|Described|p233,235-239|Mesoproterozoic|Mesoproterozoic|Amadeus Basin. Rhyolite. 1075+\-2.5 Ma age from Close et al., 2003; 1073+\-13 Ma from this study.|c. 1074 Ma|Unit of Tjauwata Group.||Overlain by Wankari Volcanics. Underlain by, or laterally equivalent to Mount Harris Basalt.|Porphyritic rhyolite.|
33811|Puntitjata Rhyolite|71210|5|Briefly described|p9|Stenian|Stenian|Correlation with the Smoke Hill Volcanics was established by Close et al., 2003a.||Tjauwata Group||Equivalent to the Smoke Hill Volcanics.||
33811|Puntitjata Rhyolite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||rhyolite|
33811|Puntitjata Rhyolite|71268|4|Described|1m_geologyp12_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin.||Unit of Tjauwata Group.|||Porphyritic rhyolite|
77236|Punuwarra suite|66256|5|Briefly described|p8, p18 Fig.14, p23-32, see comments|Stenian|Stenian|Age: early Musgravian. In southeastern part of Tjuni Purlka Tectonic Zone. More texturally and compositionally homogeneous granites. Geochemistry provided. SHRIMP whole rock Nd isotopic crystallization age.  See also p34, p36, p38, p41, p54 App.1, p66-67 App.3.|1195+/-4 Ma (GSWA).|Pitjantjatjara Supersuite||||11-JAN-17
77236|Punuwarra suite|67375|6|Mentioned|p25 Fig.17. |Mesoproterozoic|Mesoproterozoic|A-type. Early Musgrave Orogeny.||Unit in Pitjantjatjara Supersuite.||||
77236|Punuwarra suite|67553|6|Mentioned|p27-28,33|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province, North Australian Craton. Early Musgravian granite.||Unit of Pitjantjatjara Supersuite.||||
77236|Punuwarra suite|69091|5|Briefly described|p64 Fig.4.10|||||||||
77236|Punuwarra suite|69729|5|Briefly described|p74 Fig.7, p77-78|||||Pitjantjatjara Supersuite.|||A-type granites.|
23927|Purralili Sandstone|22537|6|Mentioned|42|||Parent Mahony Group||||||
23927|Purralili Sandstone|40993|4|Described|p11|||||||||
23927|Purralili Sandstone|41864|1|Redefined|p57|Frasnian||Replaces "Buchanan Sandstone" as defined 1985. Age determined by inference only.||||||
23927|Purralili Sandstone|41865|5|Briefly described|Map legend||Frasnian|||||||
23927|Purralili Sandstone|41866|5|Briefly described|Map legend|Frasnian||||||||
23927|Purralili Sandstone|42030|5|Briefly described|p750|||||||||
23927|Purralili Sandstone|44868|5|Briefly described|Map Legend||Frasnian|||||||
23927|Purralili Sandstone|64580|6|Mentioned|map legend|||Of Mahony Group.||||||15-DEC-08
23927|Purralili Sandstone|67860|4|Described|p418 Tb. 4-18, p422 fig 4-88|Frasnian|Frasnian|Eolian deposit, 0-140 m thick. Occurs as a lens near base of Glass Hill Sandstone. Type section details given. Unfossiliferous. Replaces Buchanan Sandstone. Restricted to SE Bungle Bungle Range.||Mahony Group|||Quartz sandstone.|
23927|Purralili Sandstone|68656|6|Mentioned|GEOL_LUT_CSV/500k_geologyp08_lut|Frasnian|Frasnian|||Mahony Group||||
23927|Purralili Sandstone|69165|6|Mentioned|500k_geologyp08_lut.csv|Frasnian|Frasnian|||Mahony Group||||
23927|Purralili Sandstone|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Mahony Group.||||
23927|Purralili Sandstone|71146|6|Mentioned|p33|||||||||
23927|Purralili Sandstone|71267|4|Described|GEOL_LUT_CSV files|Frasnian|Frasnian|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Mahony Group.|||Medium- to very thick-bedded, medium-grained quartz arenite|
32217|Pyramid Hill Formation|23416|5|Briefly described|Map Legend|Archean|Archean|Of Gorge Creek Group, Pilbara Craton||||||07-NOV-08
32217|Pyramid Hill Formation|23755|4|Described|p45|Archean|Archean|See also page 17 table 1. Of Gorge Creek Group.||||||15-APR-13
32217|Pyramid Hill Formation|23783|5|Briefly described|p17|||Of De Grey Group.||||||
32217|Pyramid Hill Formation|24025|4|Described|p8 Tb. 1|Archean|Archean|Of Gorge Creek Group. Shale and banded iron formation. Max. thickness: ~1000m. Geological Province: Pilbara Craton.||||||15-APR-13
32217|Pyramid Hill Formation|24184|5|Briefly described|p703, p699 Fig.3|Archean|Archean|Parent: Gorge Creek Group. Geological Province: Pilbara Craton. Overlies Cooeenia and Honeyeater Basalts disconformably||||||07-NOV-08
32217|Pyramid Hill Formation|24531|5|Briefly described|p5 Tb. 1|Archean|Archean|Of the Gorge Creek Group (Pilbara Supergroup). Geological Province: Pilbara Craton.||||||07-NOV-08
32217|Pyramid Hill Formation|24550|5|Briefly described|p31 Tb. 3.1|||Of the Gorge Creek Group. Banded iron formation. Geological Province: Pilbara Craton.||||||07-FEB-11
32217|Pyramid Hill Formation|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Of the Gorge Creek Group. Banded-iron formation.||||||07-FEB-11
32217|Pyramid Hill Formation|61253|5|Briefly described|p51|Archean|Archean|Of the Gorge Creek Group (Pilbara Supergroup). Geological Province: Pilbara Craton.||||||07-NOV-08
32217|Pyramid Hill Formation|61266|4|Described|p58 Tb.1, p60|Archean|Archean|Of the Gorge Creek Group. Conformably overlies Honeyeater Basalt. Banded iron-formation composed of centimetre-wide layers of hematitic iron and pale grey chert. Geological Province: Pilbara Craton.||||||07-NOV-08
32217|Pyramid Hill Formation|61579|5|Briefly described|p58 Fig. 2|Archean|Archean|Of the Gorge Creek Group.||||||07-NOV-08
32217|Pyramid Hill Formation|63441|5|Briefly described|p4 Tb. 1, p22|Archean|Archean|Of the Soanesville Group (Pilbara Supergroup). Conformably overlies Honeyeater Basalt; unconformably overlain by De Grey Supergroup rocks. Max. thickness: ~900m. Geological Province: Pilbara Craton. Consists of centrimetre-layered red and grey BIF.||||||07-FEB-11
32217|Pyramid Hill Formation|63538|4|Described|p6 Fig. 3|Archean|Archean|Of Soanesville Group. Underlain by Honeyeater Basalt. Geological Province: Pilbara Craton. Sedimentary rocks.||||||19-APR-13
32217|Pyramid Hill Formation|64328|5|Briefly described|p56 Tb. 1|||Of the Soanesville Subgroup (Gorge Creek Group). Shale.||||||07-FEB-11
32217|Pyramid Hill Formation|64405|5|Briefly described|p4 Fig. 3|Archean|Archean|Name inferred from Pyramid Hill only in Figure 3. Of the Soanesville Group (De Grey Supergroup). Sedimentary.||||||07-FEB-11
32217|Pyramid Hill Formation|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Unit in Soanesville Group. Banded iron-formation, chert and shale; metamorphosed.||||||
32217|Pyramid Hill Formation|66118|5|Briefly described|p148, p149 Fig.3|||Pilbara Craton. East Pilbara Terrane. Thickness: 300 m.||Top of Soanesville Group.||Unconformably overlain by Lalla Rookh Sandstone. Overlies Honeyeater Basalt in Soanesville greenstone belt.|Centimetre-layered banded iron formation.|
32217|Pyramid Hill Formation|66745|5|Briefly described|p53 Fig.3.|Mesoarchean|Mesoarchean|||Unit in Soanesville Group.||Overlies Honeyeater Basalt. Is unconformably overlain by De Grey Supergroup.|Banded iron-formation.|
32217|Pyramid Hill Formation|67130|5|Briefly described|p16|||||Soanesville Group||Overlies Honeyeater Basalt|Banded iron formation and ferruginous shale.|
32217|Pyramid Hill Formation|67197|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Soanesville Group.||||
32217|Pyramid Hill Formation|67201|5|Briefly described|p7 Fig.4|||In northern Pilbara Craton, East Pilbara Terrane.||Soanesville Group||||
32217|Pyramid Hill Formation|67668|6|Mentioned|Fig. 2; p. 154||Mesoarchean|East Pilbara Terrane, Pilbara Craton.||Soanesville Group||Overlies the Honeyeater Basalt, unconformably underlies the De Grey Supergroup.|Banded iron formation.|
32217|Pyramid Hill Formation|69015|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton. Mapped as 3 separate facies.||Of the Soanesville Group.|||Banded iron-formation, minor chert and shale; red-weathered, ferruginised, black shale; silicified shale, grey, white, and black layered chert; all metamorphosed.|02-MAY-14
32217|Pyramid Hill Formation|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Soanesville Group|||Banded iron-formation; ferruginized shale,silicified shale, shale and minor chert; metamorphosed.|
32217|Pyramid Hill Formation|69301|5|Briefly described|p5 Fig.3|||Pilbara Craton. East Pilbara Terrane.||Soanesville Group||||
32217|Pyramid Hill Formation|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Paleoarchean|Geological province: Pilbara Craton. Of Soanesville Basin. Events: Mosquito Creek Orogeny; North Pilbara Orogeny; Prinsep Orogeny; East Pilbara Terrane Rifting Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|3228-3176 Ma (inferred)|Unit of Soanesville Group.|||Banded iron-formation, ferruginised black shale, silicified shale, layered chert; all metamorphosed.|
32217|Pyramid Hill Formation|69616|5|Briefly described|p161|Archean|Archean|||Unit in Soanesville Group.||Overlies Honeyeater Basalt.||
32217|Pyramid Hill Formation|70022|6|Mentioned|p115|||East Pilbara Terrane.||Soanesville Group.||||
32217|Pyramid Hill Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Paleoarchean|Soanesville Basin.||Soanesville Group|||Banded iron-formation, chert, and shale; metamorphosed.|
32217|Pyramid Hill Formation|72668|5|Briefly described|p4-6|||East Pilbara Terrane.||Soanesville Group||Overlies the Honeyeater Basalt.|Banded-iron formation and ferruginous shale.|13-JAN-22
73868|Pyramid Well Granite|24590|5|Briefly described|p140|Archean|Archean|Age: 3310+/3Ma.||||||07-FEB-11
35670|QED Rudite|23142|5|Briefly described|p203 Fig.2|||||||||
35670|QED Rudite|60625|6|Mentioned|p48 Fig.2|||Geological Province: Eastern Goldfields.||||||26-JUN-05
35670|QED Rudite|65834|6|Mentioned|p36|||Kanowna Belle gold mine, Boorara Domain, Kalgoorlie Terrane. Mine terminology.||||Is overlain by Lowes Sandstone. Locally grades into Graves Dam Grits. Is intruded by Kanowna Belle Porphyry.|Cobble- to pebble-clast supported felsic conglomerate to breccia.|
35670|QED Rudite|70482|6|Mentioned|p324|Archean|Archean|Kanowna Belle mine, Eastern Goldfields Superterrane, Eastern Yilgarn Craton.|||||Volcaniclastics.|
35670|QED Rudite|73391|6|Mentioned|p51|||||||Is enclosed above and below by Grave Dam Grit.||
33755|Quadrio Formation|24161|5|Briefly described|p7|Cambrian|Neoproterozoic|Correlated with the Edmund Group. Age: maximum detrital zircon age of c. 700 Ma and detrital age of 511 Ma or younger. Geological Province: Edmund Basin.||||||
33755|Quadrio Formation|24183|5|Briefly described|p7|Mesoproterozoic|Mesoproterozoic|Correlated with the Edmund Group.||||||28-JUL-08
33755|Quadrio Formation|50188|2|Defined|p9, 14|Mesoproterozoic|Mesoproterozoic|Unconformably underlies Skates Hills Formation; conformable on Cornelia Sandstone. Age: c.1600Ma. Max.thickness: 1km+. Geol.Prov: Oldham Inlier.  Dominated by shale/sandstone +minor intervals of sandstone/laminated chert.||||||28-JUL-08
33755|Quadrio Formation|62453|6|Mentioned|p58|||Geological Province: Oldham Inlier.||||||
33755|Quadrio Formation|64283|5|Briefly described|p51 Fig. 2, p53|Mesoproterozoic||Geological Province: Oldham Inlier. Unconformably overlain by Skates Hills Formation; unconformably overlies Cornelia Sandstone. Age: 1.6Ga? Geological province:Oldham Inlier. Intensely silicified sandstone; steeply dipping.||||||07-FEB-11
33755|Quadrio Formation|64286|5|Briefly described|p72, p73 Fig. 1|||Formerly mapped as Cornelia Sandstone tog. with Oldham Sandstone + smaller Cornelia Formation. Geological province:Oldham Inlier. Dominantly fine-grained shaly unit with locally developed sandstone/chert intervals.Contains barite-hematite mineralisation||||||07-FEB-11
33755|Quadrio Formation|64580|4|Described|map legend||Mesoproterozoic|Shale, siltstone, chert, and minor sandstone; quartz sandstone to quartzite, and minor siltstone.||||||15-DEC-08
33755|Quadrio Formation|64772|5|Briefly described|p13, Plate 1  legend, p33|Mesoproterozoic|Mesoproterozoic|Age: <1670Ma. Listed sith Cornelia Sandstone on Plate 1. Dominantly a fine-grained shaley unit with locally developed sandstone and chert intervals; barite-hematite mineralisation is hosted in this formation. See also  p34 Fig.22, p35, p49, p50 (incl. Fig.37), p82 App.4 Tb.4.5.||||Underlies Sunbeam Group. May correlate with Scorpion Group||25-NOV-13
33755|Quadrio Formation|70826|6|Mentioned|p10|Mesoproterozoic|Mesoproterozoic|||||||
33755|Quadrio Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||shale, siltstone, sandstone, chert|
33755|Quadrio Formation|72034|6|Mentioned|500k_interpgeop16_lut|Mesoproterozoic|Paleoproterozoic|Paterson Orogen. Informally grouped with Cornelia Sandstone. |Min age~1070 Ma.||||Combined description: Shale, siltstone, chert, and minor sandstone; quartz sandstone to quartzite, and minor siltstone.|
34481|Quairading Sandstone|22769|3|Fully described|p757-58,761-63|Miocene|Early Oligocene|Basal unit of Salt River Group. Does not outcrop. Consists of grey, brown white and pink layers of sandstone, varying in size from fine to coarse sand, well rounded to subrounded, well-cemented in a clay matrix. Overlain by Yenyening Formation.||||||17-JAN-06
34481|Quairading Sandstone|65194|5|Briefly described|p123|||Lowest unit in Salt River Palaeovalley sequence. Consists of multi-coloured, fine- to coarse-grained sands, commonly cross bedded with uncertain stratigraphic position and age unknown.||||||
33438|Quartpot Pelite|22904|4|Described|p59 fig 1|Paleoproterozoic|Paleoproterozoic|Of Camel Hill Metamorphics.  Maximum depositional age c. 2025 Ma||||||07-NOV-08
33438|Quartpot Pelite|23485|4|Described|p16|Paleoproterozoic|Paleoproterozoic|Of Camel Hills Metamorphics. Geological Province: Gascoyne Complex.||||||07-NOV-08
33438|Quartpot Pelite|23486|5|Briefly described|Map Legend|Paleoproterozoic||Of Camel Hills Metamorphics. Geological Province: Gascoyne Complex.||||||07-NOV-08
33438|Quartpot Pelite|23487|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Camel Hills Metamorphics. Geological Province: Gascoyne Complex.||||||07-NOV-08
33438|Quartpot Pelite|23525|5|Briefly described|p4|||||||||
33438|Quartpot Pelite|23780|5|Briefly described|p38|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
33438|Quartpot Pelite|23781|4|Described|p33|Paleoproterozoic|Paleoproterozoic|Of Camel Hills Metamorphics.  Geological Province: Yilgarn Craton.||||||07-NOV-08
33438|Quartpot Pelite|24544|4|Described|p3|Paleoproterozoic|Paleoproterozoic|Of the Camel Hills Metamorphics. Pelitic and psammitic schist or gneiss interlayered with minor quartzite, calc-silicate gneiss and amphibolite. Age: c. 2000 Ma.||||||07-NOV-08
33438|Quartpot Pelite|50218|5|Briefly described|p241 Fig. 3, p248|Orosirian|Orosirian|Of the Camel Hills Metamorphics. Geological Province: Errabiddy Shear Zone.||||||07-FEB-11
33438|Quartpot Pelite|63866|4|Described|p158|Paleoproterozoic|Paleoproterozoic|Outcrops extensively in the Erabiddy Shear Zone. Numeric age is a SHRIMP U-Pb zircon date and is interpreted as constraining the maximum depositional age for the sedimentary protolith of this formation.|2028 +/- 5 Ma (Nelson, 2001)|Camel Hill Metamorphics|||Pelitic schist.|
33438|Quartpot Pelite|65545|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Camel Hills Metamorphics, Gascoyne Province. c. 1985 Ma. Biotite-plagio-qtz gneiss and migmatitic pelitic gneiss intruded by c. 1970 Ma sheets and veins of coarse biot trondhjemite; variable amounts biot monzogranite; minor amphib and calc-silic.||||||
33438|Quartpot Pelite|65549|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Camel Hills Metamorphics. Underlies Spring Camp Formation.  Predominantly biotite-plagioclase-quartz gneiss and migmatitic pelitic gneiss intruded by c. 1970 Ma sheets and veins of coarse-grained biotite trondhjemite.||||||08-FEB-14
33438|Quartpot Pelite|65896|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Camel Hills Metamorphics. Biotite-plagioclase-quartz(-K-feldspar-garnet-sillimanite) migmatitic pelitic gneiss;locally with chloritoid and chlorite. Shown as equivalent age to Petter Calc-silicate||||||
33438|Quartpot Pelite|66299|4|Described|p4 Fig.2, p6 Fig.3, pp95-100.|Paleoproterozoic|Paleoproterozoic|Component of Glenburgh Terrane, basement to Gascoyne Province. Possibly sourced from currently-unexposed part of proto-Dalgaringa arc.|c.2000 Ma - c.1960 Ma.|Unit in Camel Hills Metamorphics.||Faulted against Narryer Terrane units. Intruded by pluton of Moorarie Supersuite.|Pelitic diatexite and psammitic schist or gneiss interlayered with minor quartzite, calc-silicate gneiss, and amphibolite.|
33438|Quartpot Pelite|66887|4|Described|p3 Fig.2, p5 Fig.4, p6|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, southern Gascoyne Province. SHRIMP dating of detrital zircons indicate deposition after c. 2000 Ma and prior to new zircon growth at c. 1965 Ma. 177Hf/176Hf analysis of detrital zircons suggests this unit was derived from an older unit (2020-2000 Ma), currently unexposed.|c. 2000-c. 1965 Ma zircons SHRIMP|Camel Hills Metamorphics|||Includes pelitic to semipelitic schist and gneiss.|
33438|Quartpot Pelite|66950|5|Briefly described|p7, p9 Fig.8|Orosirian|Orosirian||c. 2000-1955 Ma|Of the Camel Hills Metamorphics.|||Comprises pelitic gneiss and schist.|
33438|Quartpot Pelite|67247|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, Gascoyne Province.|2001 - 1955 Ma.|Unit in Camel Hill Metamorphics.|||Biotite-plagioclase-quartz(-K-feldspar-garnet-sillimanite) gneiss and migmatitic pelitic gneiss intruded by c.1970 Ma sheets and veins of coarse-grained biotite metagranite; minor amphibolite and calc-silicate.|
33438|Quartpot Pelite|67843|3|Fully described|7-10, Throughout the article.|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane. A fore-arc deposit to the Dalgaringa continental margin arc. Mineral assemblages described in detail. SHRIMP U-Pb zircon ages are detailed. Has entirely different detrital zircon population from Petter Calc-silicate.|2031 +/- 6 Ma to 2001 +/- 26 Ma.|Unit in Camel Hills Metamorphics.|||Retrogressed pelitic schist, pelitic gneiss, pelitic diatexite; minor intercalated quartzites.|20-NOV-13
33438|Quartpot Pelite|69003|6|Mentioned|p10 Fig.10|||Fore-arc deposits to the Dalgaringa Arc.||||||
33438|Quartpot Pelite|69080|6|Mentioned|p686 Fig.4|||||||||
33438|Quartpot Pelite|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|||Camel Hills Metamorphics|||Biotite--plagioclase--quartz(--K-feldspar--garnet--sillimanite) gneiss and migmatitic pelitic gneiss intruded by c. 1970 Ma sheets and veins of coarse-grained foliated biotite metagranite; minor amphibolite and calc-silicate|
33438|Quartpot Pelite|69387|5|Briefly described|p6, p23|||Coeval with Dalgaringa Supersuite. SG and magnetic susceptibility values given.||Camel Hills Metamorphics.||||
33438|Quartpot Pelite|69583|6|Mentioned|p159 Fig.9|||||||||
33438|Quartpot Pelite|69595|6|Mentioned|p19|||Deposited in a fore-arc basin setting during the Glenburgh Orogeny. Detrital zircons range from 2080-2000 Ma. Potential source of the c. 2035 Ma peak in the Barren Basin. |2000-1959 Ma (depositional age)|Camel Hills Metamorphics||||
33438|Quartpot Pelite|70090|5|Briefly described|p453|Paleoproterozoic|Paleoproterozoic|Geological province: Gascoyne Province. Deposited between c. 2000 and 1959 Ma in a fore-arc basin setting during the Glenburgh Orogeny (Johnson et al., 2011b). Dominated by 2080-2000 Ma detrital zircons; based on Hf isotopic compositions, interpreted to be early (currently unexposed) Dalgaringa arc magmatism on thesouthern margin of the Glenburgh Terrane (Johnson et al., 2011b).||Unit of Camel Hills Metamorphics.||||
33438|Quartpot Pelite|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|100k_interpgeop_lut.csv|2001-1955 Ma||||Biotite-plagioclase-quartz(K-feldspar-garnet-sillimanite) gneiss and migmatitic pelitic gneiss intruded by sheets and veins of coarse-grained foliated biotite metagranite; minor amphibolite and calc-silicate.|
33438|Quartpot Pelite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||gneiss|
33438|Quartpot Pelite|71269|4|Described|1m_geologyp12_lut.csv|||Geological province: Gascoyne Province, Glenburgh Terrane, Capricorn Orogen, West Australian Craton. Of Gascoyne Complex.|||||Pelitic and psammitic schist or gneiss interlayered with minor quartzite, calc-silicate gneiss and amphibolite.|
33438|Quartpot Pelite|71484|5|Briefly described|p137|||Occurs west of the Padbury basin in the Errabiddy Shear Zone. Migmatised at c. 1960 Ma during Glenburgh Orogeny and contains detrital zircon ages similar to those observed from the Labouchere Formation. Possibly correlable to the Padbury Group.||Unit of Camel Hills Metamorphics.|||Medium- to high-grade pelitic and psammitic rocks.|
33438|Quartpot Pelite|73214|5|Briefly described|p974 Fig.1|Palaeoproterozoic||Glenburgh Terrane.||Camel Hill Metamorphics||||
73388|Quindalup Dunes|40400|6|Mentioned|p115|||Of McArthur and Bettany (1960).||||||
73388|Quindalup Dunes|60556|5|Briefly described|p21, p22|||Informal||||||13-NOV-07
73388|Quindalup Dunes|63330|5|Briefly described|p192, p193 Fig. 5, p194|Holocene|Holocene|Includes the Becher Suite of wetland basins. Coastal dunes, beach ridge plains, tombolos and cuspate forelands, underlain by quartzo-calcareous sand.||||||
73388|Quindalup Dunes|63454|6|Mentioned|p67|Holocene|Holocene|||||||
81674|Quinns Basalt Member|72389|5|Briefly described|Map Legend|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Gabanintha 1:100k map sheet 2644.||Singleton Formation|||Mafic volcanic rock; massive to weakly foliated; metamorphosed.|28-AUG-20
81674|Quinns Basalt Member|72494|5|Briefly described|p15-18, 21-23, 28|||Murchison Domain, Youanmi Terrane, Yilgarn Craton. Appears as Quinns Basalt member (p16) and Quinns Basalt (p22-23), its previous name. Geochemistry discussed in detail.||Singleton Formation.|||Basaltic to andesitic Fe-rich tholeiitic rocks and smaller volumes of more evolved rock types.|
77447|Quoin Formation|67354|3|Fully described|p73, pp91-93, p95 Fig.25, p103.|Sakmarian|Sakmarian|New name. Named after Quoin Island. Type section is between 1,145 m and 1,350 m in Barnett-1, and a reference section established in Blacktip-1 (Fig.23 this article). Previously included within the lower part of the Keyling Formation of Mory (1991). Shares the G. confluens Oppel-zone microflora with the underlying Treachery Formation. Probable equivalent to Keep Inlet and upper Kuriyippi Formations. Most likely deposited as a response to deglaciation of the hinterland, allowing glacially weathered material to be transported northwards into the basin. Contains reservoir quality sandstone and intraformational shales to afford seal; locally contains gas.||||Is overlain, probably unconformably, by Ditji Formation.|Basal blocky sandstone, fining upwards with thinner sandstone beds and increasing siltstones and shales; distinct and characteristic high gamma ray diamictite horizon.|
77447|Quoin Formation|69452|4|Described|p36:8, 15, 18-19|Sakmarian|Sakmarian|Gorter et al. (2008). Originally included in the Keyling Formation (Mory, 1991). Petrel Sub-basin, Bonaparte Basin. Sunsurface. Mostly fluvial following deglaciation; also intertidal, nearshore and continental deposits. Up to 750m thick. Offshore and onshore.||Kulshill Group.||Overlies Treachery Formation, probably unconformably. Is overlain by Ditji Formation, probably unconformably.|A sharp-based blocky sandstone that fines upwards into thinner beds of sandstone, siltstone and shale.|12-JUL-16
77447|Quoin Formation|69454|5|Briefly described|p38:4|Sakmarian|Sakmarian|Petrel Sub-basin, Bonaparte Basin.||Kulshill Group.||||12-JUL-16
77447|Quoin Formation|69653|6|Mentioned|p10|Cisuralian|Cisuralian|Petrel Sub-basin.||Kulshill Group.||Overlies Treachery Formation. Is overlain by Ditji Formation.||
77447|Quoin Formation|69673|5|Briefly described|p153 fig 125, p154,|Cretaceous|Toarcian|Originally called De Souza Sandstone or Hooray Sandstone. Up to 757m thick. Age derived from Palynofloras. Source rock potential. See also p154 fig 126, p159, p160, p161 p168 fig 140, p173.||Kulshill Group||Overlain by Ditji Formation, overlies Treachery Formation. Unconformably (or disconformably) overlies Poolowanna Formation.|Upwards fining sandstone, siltstone and shale.|
77447|Quoin Formation|70061|5|Briefly described|Petrel Sub-basin Figs.2 & 3, p3|Sakmarian|Sakmarian|See also Regional geology: Fig.8, p5, p11. Part of a succession (with Cape Londonderry Formation) of NW-thickening, shallow marine to fluvio-deltaic Permian and Triassic sediments across the Bonaparte Basin. Hydrocarbon reservoir.||Kulshill Group.||Overlies Treachery Formation. Is overlain by Ditji Formation.||12-JUL-16
77447|Quoin Formation|72505|5|Briefly described|p890|Asselian|Asselian|Southern Bonaparte Basin. Correlated with the P. Confluens zone.||||Overlies the Treachery Formation. Overlain by the Ditji Formation.||12-MAR-20
77447|Quoin Formation|73117|6|Mentioned|p15|Asselian|Asselian|Bonaparte Basin, southern.||Kulshill Group||Underlain by Treachery Formation. Overlain by Ditji Formation.||
22722|Race Course Plains Coquina|64449|2|Defined|p75, p79 Tb. 5, p95-97|Holocene|Holocene|Overlies; Sandfire Calcilutite. Thick: 2m. Age: 1285+/-150 yrs BP and 3625+/-260 yrs BP (see p97). Shell gravel; formed in she-string, to lensoid, to wedge-shaped deposit as chenier ridges, shoreline spits, and shoreline shell beds.||||||07-FEB-11
22722|Race Course Plains Coquina|73213|5|Briefly described|958 Fig.3(b), 961 Fig.8, 965 Fig.13|||See also p967-968.||||Overlies Lagrange Calcilutite Member (Sandfire Calcilutite).|Mobile dune sands with buried shell middens.|19-JAN-23
74819|Racecourse Tonalite|64891|5|Briefly described|p37 Fig. 2, p41, p50-51 Tb. 1|Archean|Archean|Of Cullculli Suite (Annean Supersuite). Age: 2760+/-8Ma. Geological province: Murchison Domain. Tonalite; metamorphosed.||||||07-FEB-11
74819|Racecourse Tonalite|67129|5|Briefly described|p19 Fig.20|Archean|Archean|Murchison Domain, Youanmi Terrane.||Annean Supersuite.|||Syn-volcanic tonalitic rocks.|
74819|Racecourse Tonalite|69583|5|Briefly described|p49, p52; Plate 2|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Cullculli Suite.|||Metagranite.|
74819|Racecourse Tonalite|69584|5|Briefly described|p5 Fig.2|Neoarchean|Neoarchean|||CullCulli Suite|||Tonalite.|
74819|Racecourse Tonalite|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Cullculli Suite.||||
74819|Racecourse Tonalite|70796|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Younami Terrane.|2760 +/ 5 Ma to 2750+/ 5 Ma (isotopic)|Cullculli Suite|||Metagranite, undivided; metamorphosed; includes deeply weathered rock.|
74819|Racecourse Tonalite|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv.|2770+\-5, 2760+\-5 Ma|Unit of Cullculli Suite.|||Metagranite, undivided; metamorphosed; includes deeply weathered rock|
74819|Racecourse Tonalite|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.||Cullculli Suite.|||Metatonalite (section only); metagranite, includes deeply weathered rock.|
74819|Racecourse Tonalite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Youanmi Terrane.|Max age 2760 +/-5 Ma, min 2750 +/-5 Ma.||||Metagranite, undivided; metamorphosed; includes deeply weathered rock.|
33977|Radigans Yard Granodiorite|22547|6|Mentioned|p17|||||||||
33977|Radigans Yard Granodiorite|50437|6|Mentioned|p4.2|||Geological Province: Kimberley Region. Of the Kevins Dam Suite.||||||
31687|Radio Hill Intrusion|24353|5|Briefly described|p9 Fig.5|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
31687|Radio Hill Intrusion|43822|5|Briefly described|map legend|Archean|Archean|Layered mafic intrusions approx. 2925 Ma. Of Pilbara Supergroup.||||||07-NOV-08
31687|Radio Hill Intrusion|63441|5|Briefly described|p12 Tb. 2, p38|Archean|Archean|Of the Radley Suite. Mafic layered intrusion. Mined for nickel and copper.||||||07-FEB-11
31687|Radio Hill Intrusion|64174|5|Briefly described|Map legend|Archean|Archean|Part of the Radley Suite (Sisters Supersuite). Age : c.2929Ma. Gabbro, pyroxenite, and minor peridotite; metamorphosed.||||||07-NOV-08
31687|Radio Hill Intrusion|64580|4|Described|map legend||Mesoarchean|Of Radley Suite. Gabbro, pyroxenite, and minor peridotite; metamorphosed.||||||15-DEC-08
31687|Radio Hill Intrusion|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological Province: West Pilbara Granite-Greenstone Terrane, Central Pilbara Tectonic Zone, and southwest Pilbara inlier, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 2925 Ma|Unit of Radley Suite.|||Gabbro, pyroxenite, and minor peridotite; metamorphosed|
31687|Radio Hill Intrusion|69299|6|Mentioned|p12|||c. 2925 Ma mafic-ultramafic Maitland and Radio Hill intrusions|c. 2925 Ma||||Ultramafic.|
31687|Radio Hill Intrusion|70775|5|Briefly described|p37, p66, p78-p79|Mesoarchean|Mesoarchean|The basal ultramafic layer contains massive, disseminated, veind and brecciated pyrrhotite and pentlandite-chalcopyrite-magnetite at or near the contact with the Nallana Formation.|c. 2925 Ma|Radley Suite|||Basal ultramafics consisting of lherzolite, dunite and websterite overlain by a gabbroic zone including quartz gabbro, gabbro and gabbronorite.|
31687|Radio Hill Intrusion|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||gabbro, dolerite, anorthosite|
31687|Radio Hill Intrusion|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||2929+/-13 Ma|Radley Suite|||Gabbro, pyroxenite, and minor peridotite; metamorphosed.|
68740|Radley Suite|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Of the Sisters Supersuite. Ultramafic layered intrusions.  Geological Province: western and central Pilbara Craton.||||||07-NOV-08
68740|Radley Suite|63441|5|Briefly described|p12 tb. 2, p38|Archean|Archean|Of the Sisters Supersuite. Contains 7 named intrusions including Yannery Granite. Age: 2930-2925Ma. Geological province: Pilbara Craton. Mafic to ultramafic layered intrusions. See also p33 Fig. 12.||||||07-FEB-11
68740|Radley Suite|63538|6|Mentioned|p6 Fig. 3|Archean|Archean|Geological Province: Pilbara Craton.||||||19-APR-13
68740|Radley Suite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Sisters Supersuite. Contains 7 named intrusions and Yannery Granite  Ages for constituents: c.2930Ma, c.2929Ma,c.2925Ma and c.2931Ma.||||||07-NOV-08
68740|Radley Suite|64580|6|Mentioned|map legend|||||||||
68740|Radley Suite|66217|5|Briefly described|p43.|||western part of the East Pilbara Terrane. Hosts PGE and Ni-Cu mineralisation.||Sisters Supersuite.|||Layered mafic-ultramafic intrusions.|10-JUN-20
68740|Radley Suite|67201|4|Described|p7 Fig.4, p13 Fig.8, p16-17 Fig.9, p23|||West Pilbara Superterrane.|c. 2925 Ma|Sisters Supersuite|Yannery Granite||Ultramafic intrusions.|
68740|Radley Suite|69185|5|Briefly described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Sisters Supersuite.|Includes Dingo Intrusion, Maitland Intrusion, Mount Sholl Intrusion, Munni Munni Intrusion, North Whundo Intrusion, Radio Hill Intrusion, Sherlock Intrusion, Yannery Granite.|||
68740|Radley Suite|69301|5|Briefly described|p5 Fig.3|||Pilbara Craton. West Pilbara Superterrane.|||||Granitic rocks.|
68740|Radley Suite|70022|6|Mentioned|p115|||West Pilbara Superterrane.||||||
68740|Radley Suite|70775|4|Described|iii, p13, p15|Mesoarchean|Mesoarchean|Hosts Ni-Cu and PGE mineralization formed as part of layered ultramafic-mafic intrusions. See also p29 tbl 5, p42, p64-p66, p72, p78.|c. 2930-2924 Ma (Sun and Hoatson, 1992)|Sisters Supersuite|Includes the Yannery Granite and the Munni Munni Intrusion.||Ultramafic layers of dunite, peridotite and pyroxenite overlain by a layered mafic section of gabbro, leucogabbro, norite and more rarely anorthosite and granophyre.|
68740|Radley Suite|72034|6|Mentioned|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Mount Sholl Intrusion, North Whundo Intrusion, Yannery Granite, Munni Munni Intrusion, Radio Hill Intrusion, Dingo Intrusion, Maitland Intrusion.|||
68740|Radley Suite|72668|5|Briefly described|p4, p15, p17, p21-22|||West Pilbara Superterrane.|c. 2925 Ma|Sisters Supersuite|||Ultramafic to mafic intrusions.|
78756|Raeside Granite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2760 +/- 4 Ma - 2753 +/- 6 Ma (isotopic).||||Monzogranite to tonalite; locally gneissic.|
78756|Raeside Granite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2760+\4 Ma; 2753+\-6 Ma||||Monzogranite to tonalite; locally gneissic|
28948|Ragged Range Conglomerate|13194|4|Described|p394 Tb. 4-16, p402 fig 4-66|Frasnian|Frasnian|Type Section: Conglomerate Hill 16o24'S 128o21E. 290-600m thick alluvial fan deposits. [Stratigraphic details contradictory].||||Overlies Kununurra Formation (conformably) at Matheson Ridge. Overlain by Cyril Sandstone (conformably).|Red conglomerate, pebbly sandstone and sandstone.|
28948|Ragged Range Conglomerate|23821|4|Described|p245|Devonian|Devonian|Geological Province: Ord Basin.||||||
28948|Ragged Range Conglomerate|32870|6|Mentioned|Fig.6|||Refers Kaulback & Veevers (1969).||||||27-NOV-06
28948|Ragged Range Conglomerate|40993|6|Mentioned|p4|||||||||
28948|Ragged Range Conglomerate|41158|6|Mentioned|p40|||See also p41.||||||27-NOV-06
28948|Ragged Range Conglomerate|41864|1|Redefined|p49|||||||||
28948|Ragged Range Conglomerate|41865|5|Briefly described|Map legend|Frasnian||||||||
28948|Ragged Range Conglomerate|42030|5|Briefly described|p749|||||||||
28948|Ragged Range Conglomerate|42191|6|Mentioned|Fig.8 P442|||||||||
28948|Ragged Range Conglomerate|44230|5|Briefly described|Map Legend||Frasnian|||||||
28948|Ragged Range Conglomerate|45038|14|Not recorded|p.26 Fig 71|||Abbreviation of Ragged Range Conglomerate Member?||||||27-NOV-06
28948|Ragged Range Conglomerate|45039|6|Mentioned|p16|||Upper Devonian||||||
28948|Ragged Range Conglomerate|45047|6|Mentioned|p105|||||||||
28948|Ragged Range Conglomerate|45058|6|Mentioned|Fig. 3|||L.Cambrian||||||
28948|Ragged Range Conglomerate|60006|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Geological Province: Bonaparte Basin. Of Cockatoo Group. Sandstone, polymict conglomerate.||||||
28948|Ragged Range Conglomerate|60682|4|Described|p22 Table 5, 23|Frasnian|Frasnian|Of Cockatoo Group. Previously Ragged Range Conglomerate Member. Unconformably overlies Whitewater Volcanics and Antrim Plateau Volcanics. Overlain by Kellys Knob Sandstone. Thickness: >300m. Geological Province: Bonaparte Basin. Sandstone and conglomerate||||||12-DEC-06
28948|Ragged Range Conglomerate|64580|6|Mentioned|map legend|||Of Cockatoo Group.||||||15-DEC-08
28948|Ragged Range Conglomerate|65331|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of Cockatoo Group, Bonaparte Basin. Sandstone, polymict conglomerate||||||
28948|Ragged Range Conglomerate|69165|6|Mentioned|500k_geologyp08_lut.csv|Frasnian|Frasnian|||Cockatoo Group||||
28948|Ragged Range Conglomerate|69452|4|Described|p36:6, 9-10|Frasnian|Frasnian|Veevers and Roberts (1968). Equivalent to Ragged Range Conglomerate Member (Plumb, 1968). Petrel Sub-basin, Bonaparte Basin. Onshore. Up to c.300m thick. Alluvial fan to shallow tidal environments of deposition, proximal to uplifted Proterozoic rocks. Contains pelecypods and gastropods.||Cockatoo Group.||Unconformably overlies Antrim Plateau Volcanics and Whitewater Volcanics. It is conformably overlain by, and interfingers with, Kellys Knob Sandstone.|Flat-lying beds of polymictic conglomerate and red-brown sandstone with occasional cross-beds; conglomerate clasts are up to cobble-boulder size and set in a sandy matrix.|11-JUL-16
28948|Ragged Range Conglomerate|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Cockatoo Group.||||
28948|Ragged Range Conglomerate|69673|5|Briefly described|p169, p169 fig 140|Frasnian|Frasnian|Up to 300m thick.||Cockatoo Group||Overlain by Kellys Knob Sandstone|Polymictic conglomerate and sandstone.|
28948|Ragged Range Conglomerate|70206|5|Briefly described|Map Legend|Devonian|Devonian|Bonaparte Basin.||Unassigned Cockatoo Group|||Sandstone, polymictic conglomerate.|
28948|Ragged Range Conglomerate|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, conglomerate|
78530|Railway Dam Metagranodiorite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||3010 - 2600 Ma (inferred).||||Foliated biotite-bearing metagranodiorite.|
78530|Railway Dam Metagranodiorite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|3010-2600 Ma (inferred)||||Foliated biotite-bearing metagranodiorite|
68669|Railway Supersuite|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Age: 3130-3114Ma. Geological Province: Pilbara Craton.  See also p54-55 Fig. 3.||||||07-NOV-08
68669|Railway Supersuite|63441|4|Described|p35, p10 Tb. 2|Archean|Archean|Includes Pinnacle Hill Gneiss and Twin Table Monzogranite. Contains some of the oldest components of Cherratta Granitic Complex. Age: 3130-3110Ma. In the Sholl Terrane, West Pilbara Superterrane/Pilbara Craton. See also p32 Fig. 11.||||||07-FEB-11
68669|Railway Supersuite|63538|6|Mentioned|p2 Fig. 1, p5, p6 Fig. 3|Archean|Archean|Geological Province: Pilbara Craton.||||||19-APR-13
68669|Railway Supersuite|64174|5|Briefly described|Map legend|Archean|Archean|Includes Pinnacle Hill Gneiss and Twin Table Monzogranite.  Age range includes: 3130-3114Ma, 3123-3114Ma and c.3093Ma. Geological province: Sholl Terrane, West Pilbara Superterrane.||||||07-NOV-08
68669|Railway Supersuite|64580|4|Described|map legend||Mesoarchean|Gneissic metamonzogranite; locally migmatitic, and veined by younger granitic rocks; locally contains large mafic and ultramafic xenoliths.||||||15-DEC-08
68669|Railway Supersuite|64632|6|Mentioned|p201 Fig.1|Mesoarchean|Mesoarchean|Sholl Terane, West Pilbara Superterrane. Coeval with Whundo Group.||||||
68669|Railway Supersuite|66118|5|Briefly described|p146 Fig.1|||Pilbara Craton. West Pilbara Superterrane. Sholl Terrane.|c. 3120 Ma Whundo Group and Railway Supersuite|||||
68669|Railway Supersuite|66217|5|Briefly described|p9.|Mesoarchean|Mesoarchean|Sholl Terrane.|3.13-3.11 Ga.|||||
68669|Railway Supersuite|67201|4|Described|p7 Fig.4, p11, p13 Fig.8, see comments|Archean|Archean|In northwestern Pilbara Craton, Sholl Terrane, West Pilbara Superterrane. Age: 3130-3114 Ma (Van Kranendonk et al. 2006). Page location continued: p18, p23, p26, p67.|3130-3110 Ma||Twin Table Monzogranite, Bullock Hide Intrusion, Pinnacle Hill Gneiss.|Intrudes Cheratta Granitic Complex, and lower stratigraphic levels of Whundo Group. Is intruded by Elizabeth Hill Supersuite (Cliff Pool Tonalite).|Metatonalite, metagranodiorite, and metamonzogranite gneiss.|24-NOV-16
68669|Railway Supersuite|68035|5|Briefly described|p289, p290 Fig 5|Mesoarchean|Mesoarchean|Sholl Terrane|3130 - 3090 Ma||||Granitic and mafic rocks.|
68669|Railway Supersuite|69185|5|Briefly described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.|||Includes Pinnacle Hill Gneiss, Twin Table Monzogranite.|||
68669|Railway Supersuite|69301|4|Described|p5 Fig.3, p14|||Pilbara Craton. West Pilbara Superterrane. Sholl Terrane. Age: oldest zircons are 3149+/-15 Ma, and Nd TDM model ages are 3.23-3.21 Ga (Smithies et al. 2007a).|3.13-3.11 Ga, see comments.||||Granitic rocks. Composed of metatonalite, metagranodiorite, and metamonzogranite gneiss.|
68669|Railway Supersuite|70022|6|Mentioned|p114-115|||Sholl Terrane, West Pilbara Superterrane.|3130-3090 Ma.|||||
68669|Railway Supersuite|70775|5|Briefly described|p8 fig 5, p9, p13|Mesoarchean|Mesoarchean|Sholl Terrane. The upper age of 3130 +/- 4 Ma was derived from Nelson 1999e. Geochemsitry briefly discussed. See also p15-p17, p25, p32-p38, p41, p44 fig 27, p53, p64, p70, p75, p81.|c. 3130-3093 Ma (Van Kranendonk et al., 2006)||Includes the Pinnacle Hill Gneiss, Bullock Hide Intrusion and the Twin Table Monzogranite.|Faulted against the Whundo Group. Intruded by the Maitland River Supersuite.|Tonalite, granodiorite, monzogranite and at least one large ultramafic-mafic intrusion.|
68669|Railway Supersuite|70826|6|Mentioned|p8|Mesoarchean|Mesoarchean|Karratha Terrane. ||||Intrudes the Whundoo [sic, should be Whundo] Group.||13-MAY-20
68669|Railway Supersuite|71349|6|Mentioned|p738|Archean|Archean|Sholl Terrane. Coeval with Whundo Group.|c.3.1 Ga.|||||
68669|Railway Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||Max age 3130+/-4 Ma, min 3093+/-4 Ma.||Includes Twin Table Monzogranite, Pinnacle Hill Gneiss, Bullock Hide Intrusion.||Metatonalite, metagranodiorite, and metamonzogranite; gneissic and with greenstone xenoliths; local ultramafic--mafic intrusive rocks.|
68669|Railway Supersuite|72251|6|Mentioned|p52|Mesoarchean|Mesoarchean|Geological province: Sholl Terrane, West Pilbara Superterrane, Pilbara Craton.|3130-3090 Ma|||||
68669|Railway Supersuite|72668|5|Briefly described|p3-4, p12-13, p16, p28|||Cheratta Granitic Complex, Sholl Terrane of the West Pilbara Superterrane. Granitic gneisses and monzogranite are contemporaneous with the Whundo Group.|c. 3130-3090 Ma|||Coeval with the Whundo Group.|Granitic gneisses and monzogranite.|13-JAN-22
39886|Rainbow Suite|24596|6|Mentioned|p561|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
34926|Rainy Rocks Monzogranite|22902|5|Briefly described|68|||Age 2678 +- 14 Ma||||||
34926|Rainy Rocks Monzogranite|24306|5|Briefly described|p943|Archean|Archean|Age: 2678 +/- 14Ma.   Geological Province: Yilgarn Craton||||||07-NOV-08
72411|Rapide Granite|62633|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region - Aileron Province. Garnet bearing biotite granite, mostly porphyritic with tabular feldspars, sometimes defining a weak foliation.||||||07-NOV-08
72411|Rapide Granite|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Of Carrington Suite. Garnet-bearing biotite granite, mostly porphyritic with tabular feldspars, weak to strong foliation; may include banded gneiss.||||||15-DEC-08
72411|Rapide Granite|65332|5|Briefly described|Map Legend|Palaeoproterozoic|Palaeoproterozoic|Shown as equivalent age to Carrington Suite, younger than 1805 Ma Stafford Event. Garnet-bearing biotite granite, mostly porphyritic with tabular feldspars, locally defining a weak foliation||||||
72411|Rapide Granite|69427|5|Briefly described|p12:3, 30-31, 33|Statherian|Statherian|Edgoose et al. (in prep.). Poor, extensive outcrops E of Lake Mackay, Aileron Province. May have been generated by granulite-facies partial melting of a metasedimentary succession. SHRIMP U-Pb zircon tentative magmatic age, isotopically disturbed at 1590 Ma.|1760 Ma (Kinny, 2002).||||Leucocratic, typically undeformed garnet-bearing granite and syenogranite, locally with coarse tabular K-feldspar; peraluminous, locally contains minor amounts of orthopyroxene or spinel +/- corundum.|12-JUL-16
72411|Rapide Granite|69508|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province.||Carrington Suite.|||Garnet-bearing biotite granite, mostly porphyritic with tabular K-feldspar, sometimes defining a weak foliation.|
72411|Rapide Granite|69794|5|Briefly described|iv, p1, p6-9|Statherian|Statherian|Geological province: Aileron Province. Of Arunta region. Weakly porphyritic. Sample NTGS LM01CJE006 (biotite granite) yielded a magmatic crystallisation age of 1615+\-6 Ma, which matched felsic intrusives exposed in the Warumpi Province, and the Ennugans Mountains Granite (NTGS NB11EEB319A; Kositcin et al 2013). Metamorphic zircon rims dated at c. 1578 Ma indicate age of metamorphism, consistent with c. 1590-1560 Ma Chewnings Event. Previously dated at c. 1760 Ma by Kinny (2002).||||||06-APR-20
72411|Rapide Granite|70826|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|Intruded during intracratonic reactivation of the Capricorn Orogen.||||||
72411|Rapide Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
72411|Rapide Granite|71592|5|Briefly described|Appendix A.|||Arunta Orogen. Metamorphosed at 1578 +7.1/-2.5 Ma.|1615+/-6 Ma (U-Pb zircon SHRIMP)||||Granite.|
72411|Rapide Granite|71858|5|Briefly described|p2, p55|Statherian|Statherian|Aileron Province. Outcrops on the LAKE MACKAY map sheet.|1615 +/- 6 Ma (Kositcin et al, 2014)|||||
72411|Rapide Granite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Orogen.||Carrington Suite|||Garnet-bearing biotite metagranite, mostly porphyritic with tabular feldspars; weak to strong foliation; may include banded gneiss.|
78517|Rason gneiss|68107|5|Briefly described|p617|Neoarchean|Neoarchean|NE Yilgarn; east of the Yamarna Shear Zone.|2706 +/- 22 Ma (Cassidy 2007).||||Granite gneiss.|22-SEP-14
22731|Ravelstone Formation|7161|6|Mentioned|p94|||Glengarry Basin.||||Stratigraphic equivalent of the Thaduna Greywacke and Johnson Cairn Shale.||02-MAY-12
22731|Ravelstone Formation|12099|4|Described|p676, p677-8 Figs.2 & 4, p680-1, p685|Orosirian|Orosirian|New or redefined unit by Occhipinti et al. (1997). Formerly considered part of the Thaduna Greywacke. Deposited from turbidity currents. Detrital zircons give maximum depositional age of c.2014 Ma.|2014 +/- 22 Ma (Nelson, 1997).|Unit in Bryah Group.||Disconformably overlies Karalundi Formation. Is unconformably overlain by Bangemall Group. Is conformably overlain by Horseshoe Formation.|Succession of graded layers of lithic and quartz wacke, shale and siltstone. Contains lenses of chert in the north.|04-MAR-13
22731|Ravelstone Formation|22493|6|Mentioned|p94|||||||||
22731|Ravelstone Formation|22694|5|Briefly described|p7|||Bryah Group, formerly Thaduna Greywacke||||||
22731|Ravelstone Formation|22940|4|Described|p15, Fig.1 p3|Paleoproterozoic|Paleoproterozoic|U-Pb zircon age 2014+/-22 Ma (Nelson, 1997). Formerly part of Thaduna Fm. See also Fig.6 p14, Table 2 p12. of Bryah Group.||||||07-NOV-08
22731|Ravelstone Formation|23153|5|Briefly described|p83|||previously part of Thaduna Greywacke.||||||
22731|Ravelstone Formation|23592|5|Briefly described|p10|Paleoproterozoic|Paleoproterozoic|Age: 2014+/-22 Ma (U-Pb SHRIMP). Of Bryah Group. Geological Province Bryah Basin.||||||07-NOV-08
22731|Ravelstone Formation|23593|5|Briefly described|p2 Fig 1|||Of Bryah Group. Geological Province: Bryah Basin||||||
22731|Ravelstone Formation|23600|5|Briefly described|p4 Fig 2|||Of Bryah Group. Geological Province: Bryah Basin.||||||
22731|Ravelstone Formation|23744|5|Briefly described|p10 Table 1|Paleoproterozoic|Paleoproterozoic|Age: 2014+/-22 Ma. Of Bryah Group. Geological Province: Bryah Basin.||||||07-NOV-08
22731|Ravelstone Formation|23747|4|Described|p13|Paleoproterozoic|Paleoproterozoic|Age: 2014+/-22 Ma (U-Pb SHRIMP). See also page 9, page 4 table 1. Previously part of Thaduna Greywacke. Of Bryah Group. Geological Province: Bryah Basin.||||||07-NOV-08
22731|Ravelstone Formation|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Bryah Group. Geological Province: Bryah Basin||||||
22731|Ravelstone Formation|23749|5|Briefly described|p3 table 1|Proterozoic|Proterozoic|Of Bryah Group. Geological Province: Bryah Basin.||||||
22731|Ravelstone Formation|23795|5|Briefly described|p3|Proterozoic|Proterozoic|Geological Province: Glengarry Basin.||||||
22731|Ravelstone Formation|23890|5|Briefly described|p21 Fig.11|||Of Bryah Group. Geological Province: Bryah Basin.||||||
22731|Ravelstone Formation|24021|5|Briefly described|p3, Fig. 1|||Parent: Bryah Group.||||||
22731|Ravelstone Formation|43830|5|Briefly described|Map Legend||Paleoproterozoic|Bryah Basin||||||07-NOV-08
22731|Ravelstone Formation|49893|6|Mentioned|p2 Fig.1|||Of the Bryah Group.||||||
22731|Ravelstone Formation|49896|5|Briefly described|p3 Tb. 2|||Of the Bryah Group. Max. Age: 2014+/-22Ma.||||||
22731|Ravelstone Formation|50222|4|Described|p320 Fig. 3, p325|Paleoproterozoic|Paleoproterozoic|Of Bryah Group.  Graded beds of  wacke, shale and siltstone.  Unconformably overlain by Bangemall Group (in north).  Disconformably overlies Narracoota Fm.  Age: <2.0Ga (SHRIMP:  Nelson, 1997). Max. thickness: 1000m.  Geol. Prov: Bryah Basin.||||||07-NOV-08
22731|Ravelstone Formation|50226|5|Briefly described|p421 Fig. 4, p422|||Of the Bryah Group.  Overlies the Narracoota Formation.  Geological Province: Bryah Basin.||||||
22731|Ravelstone Formation|61271|6|Mentioned|p105 Fig.1, p107|||Of the Bryah Group.||||||
22731|Ravelstone Formation|61848|5|Briefly described|p300|||Turbiditic metasedimentary rocks, BIF and associated clastic sediments. Geological Province: Bryah Basin.||||||03-JUL-06
22731|Ravelstone Formation|62289|6|Mentioned|p4 Fig. 2|Palaeoproterozoic|Palaeoproterozoic|Of Bryah Group. Geol Prov: Bryah Basin. Occhipinti et al. (1997); Parajina et al. (1998c) and this study.||||||
22731|Ravelstone Formation|63866|5|Briefly described|p164||Orosirian|Western Glengarry Basin. SHRIMP age likely represents the maximum depostional age for this unit and the Bryah Group.|2014 +/- 22 Ma (SHRIMP U-Pb, Nelson, 1996)|Bryah Group||||
22731|Ravelstone Formation|64580|4|Described|map legend||Paleoproterozoic|Of Bryah Group. Chert; Lithic wacke and siltstone; turbiditic.||||||09-DEC-08
22731|Ravelstone Formation|64724|5|Briefly described|p43|Orosirian|Orosirian|||Of Bryah Group.||||02-APR-12
22731|Ravelstone Formation|65408|5|Briefly described|pp82-83.|Paleoproterozoic|Paleoproterozoic|||Unit in Bryah Group.|||Turbiditic sedimentary rocks: quartz-lithic wacke.|21-JAN-22
22731|Ravelstone Formation|65411|5|Briefly described|p90, p91.|Paleoproterozoic|Paleoproterozoic|||Unit in Bryah Group.|||Lithic wacke.|
22731|Ravelstone Formation|65412|6|Mentioned|p97 Fig.1.|Paleoproterozoic|Paleoproterozoic|||||||
22731|Ravelstone Formation|65419|2|Defined|p4 Fig.1, p25, pp34-35, p39.|Paleoproterozoic|Paleoproterozoic|Type area outcrops 12 km north of the Fortnum turnoff along the Peak Hill road. Age from galena veins, reported by J. Richards (in Gee, 1990), which he had attributed to the Thaduna Greywacke. Units assigned to Thaduna Greywacke (now part of the Yerrida Group) west of the Great Northern Highway on the  Peak Hill 1:250 000 sheet are now assigned to this unit. Includes detrital zircons of uncertain provenance aged 2014 +/- 22 Ma (Nelson, 1997). Thickness uncertain, possibly c.1000 m.|1900 Ma (Pb-Pb isochron).|Unit in Bryah Group.||Conformably overlies and interdigitates with Narracoota Formation. In faulted contact with Peak Hill Schist. Is overlain conformably and gradationally by the Horseshoe Formation.|Predominantly grey, medium-grained lithic and quartz wacke, shale and siltstone.|
22731|Ravelstone Formation|65896|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Bryah Group. Ferruginous lithic wacke and siltstone; chloritic fragments; graded beds (locally coeval and interbedded with Narracoota Formation); metamorphosed.||||||
22731|Ravelstone Formation|65913|6|Mentioned|p2 Fig.1. |||||Unit in Bryah Group.||||
22731|Ravelstone Formation|66112|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Bryah Group. Lithic wacke and siltstone; chloritic fragments; graded beds (coeval and interbedded with Narracoota Formation). Includes  unnamed unit of lithic quartz-feldspar sandstone; interbedded minor siltstone; thinly bedded, chloritic matrix.||||||
22731|Ravelstone Formation|66427|6|Mentioned|p40 Fig.1|||||Unit in Bryah Group.||||
22731|Ravelstone Formation|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic|||Bryah Group|||Lithic wacke and siltstone; turbiditic|
22731|Ravelstone Formation|69003|4|Described|p11-14|||Bryah Basin. 1000m thick. Rift-fill succession.|c.2010 Ma (maximum deposition age).|Bryah Group.||Conformably overlies Narracoota Formation. Is overlain conformably by Horseshoe Formation.|Turbidites.|
22731|Ravelstone Formation|69010|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Bryah Basin. An unnamed sub-unit is mapped separately: lithic quartz-feldspar sandstone, interbedded minor siltstone, thinly bedded with chloritic matrix.|2014-1983 Ma|Of the Bryah Group.|||Comprises lithic wacke and siltstone; chloritic fragments; graded beds.|24-APR-14
22731|Ravelstone Formation|69028|6|Mentioned|Map Legend|Orosirian|Orosirian|Bryah Basin.|c.2000 Ma|||Coeval and interbedded with the Narracoota Formation.||06-MAY-14
22731|Ravelstone Formation|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|||Bryah Group||Coeval and interbedded with Narracoota Formation|Lithic wacke and siltstone; chloritic fragments; graded beds, lithic quartz-feldspar sandstone, interbedded minor siltstone; thinly bedded; chloritic matrix.|
22731|Ravelstone Formation|69583|5|Briefly described|Plate 2|||Bryah Basin. Coeval with Narracoota Formation.||||Interbedded with Narracoota Formation.||
22731|Ravelstone Formation|69596|5|Briefly described|p10-11|||Bryah Basin.||||Disconformably overlies Narracoota Formation. Is overlain conformably by Horseshoe Formation.|Turbiditic siliciclastic rocks.|
22731|Ravelstone Formation|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|West Australian Craton,  West Australian Craton, Bryah Basin|2014-1920 Ma|Bryah Group|||Lithic wacke and siltstone, lithic quartz-feldspar sandstone; interbedded minor siltstone that is thinly bedded with a chloritic matrix.|
22731|Ravelstone Formation|70796|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|Bryah Basin, Capricorn Orogen.|2014 +/ 22 Ma to 1920 Ma (isotopic/inferred)|Bryah Group, upper|||Lithic wacke and siltstone; chloritic fragments; graded beds.|
22731|Ravelstone Formation|70804|4|Described|p2, p6-p9, p16, p24, p26|||Bryah Basin. Poorly exposed in scattered low outcrops over a wide area in the northern and central parts of the basin. Rocks assigned to this unit were previously considered by Macleod (1970) and Gee (1979, 1987) to belong to the Thaduna Greywacke. Deposited as turbidity currents. Contact with the Narracoota Formation is exposed in a riverbed about 1km due east of the Fortnum-Peak Hill turn off [description provided on p16]. See also p28, p37-p38, p41-p42, plate 1.||Bryah Group||Disconformably overlies and locally interfingers with the Narracoota Formation. Conformably overlain by the Horseshoe Formation. Unconformably overlain by the Bangemall Group.|Lithic and quartz wacke, shale and siltstone.|
22731|Ravelstone Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||greywacke, sandstone|
22731|Ravelstone Formation|71269|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen, West Australian Craton. Of Bryah Basin. Events: Capricorn Orogeny (1817-1772 Ma); Glenburgh Orogeny (2002-1947 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv.|2014-1920 Ma (inferred)|Unit of Bryah Group.|||Lithic wacke and siltstone; chloritic fragments; graded beds|
22731|Ravelstone Formation|71468|5|Briefly described|p24-25|Orosirian|Orosirian|Geological province: Capricorn Orogen, Yilgarn Craton. Of Bryah Sub-basin.||||Overlain by Horseshoe Formation. Laterally grades into, and underlain by Narracoota Formation.||
22731|Ravelstone Formation|71484|4|Described|p123,125,128,134-136|Orosirian|Orosirian|Geological province: Of Bryah Basin. Only exposed in the N Bryah Basin, and does not appear to be present in the south. Intensely deformed to felsic schist, or quartz-sericite schist. Interpreted maximum depositional age of 2014+\-22 Ma, overlapping with, or younger than c. 2000 Ma dolerites in the Narracoota Formation. Represent last phase of volcanism and volcanosedimentary deposition near the end of Bryah Basin development.|c. 2014 Ma|Unit of Bryah Group.||Overlain by Horseshoe Formation. Underlain by, and interfingers with Narracoota Formation.|Lithic wacke and siltstone; chloritic fragments; graded beds.|30-AUG-19
22731|Ravelstone Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Bryah Basin.|Max age 2014+/-22 Ma, min ~1920 Ma|Bryah Group, upper|||Lithic wacke and siltstone; chloritic fragments; graded beds.|
78594|Ravensthorpe Suite|65487|4|Described|p6|Mesoarchean|Mesoarchean|Ravensthorpe Terrane nomenclature abandoned. Contains the comagmatic Annabelle Volcanics and Manyutup Tonalite.  Metamorphosed between 400-600 degC and approx. 2.5 kbar. Age of 2966 +/- 12 Ma (Savage et al., 1996) from Manyutup Tonalite. Cut by numerous mafic dykes of Gnowangerup-Fraser, Nindibillup and Beenong Dyke Suites.||||||16-JAN-14
80304|Rawlinna Member|70771|4|Described|p4-5, p60-p61|Miocene|Miocene|Eucla Platform, Eucla Basin. Informal name, referred to frequently as the 'upper member of the Nullarbor Limestone'. This unit is highly fossiliferous, containing abundant fragmented echinoids, foraminfers, coralline algae and bivalves, gastropods, serpulid worm tubes, bryozoans and scleractinian corals. Deposited extensively across the Eucla Platform, this unit covers approximately 120, 000 square kilometers. maximum depositional thickness is indeterminate; however, drillhole logs suggest that it exceeds 50m in parts. Interpreted to have been deposited across a broad open shelf, characterised by good circulation, normal marine salinities and water depths ranging from 30-45m.||Nullarbor Limestone||Overlies the Mullamullang Member. Equivalent to (grades laterally into) the Colville Sandstone.|Highly fossiliferous limestone ranging from lime mudstone textures to rudstone textures.|31-JAN-18
74139|Razorback Chert|60636|4|Described|p46, p54|Archean|Archean|Of Warrawoona Group - newly named after the Box Soak Razorback. Consists of (grey-)black and white banded cherts, occasionally grading into grey-green massive chert. Overlain by Duffer Formation. Max. thick: ~30.||||||07-FEB-11
74139|Razorback Chert|62427|5|Briefly described|p5,p11 Fig.7, p13 Fig.10, p13-14,p16-17 |||Informal name for the oldest preserved chert unit of this Group E of the Box Soak Fault; deformed.||Of the Warrawoona Group||Is overlain by Duffer Formation. Correlated with McPhee Chert.|Grey-black and white banded chert occasionally grades into grey-green massive chert and has a maximum thickness of ~30m.|
68498|Rea Dacite|63441|2|Defined|p10 Tb. 2, p36|Archean|Archean|Of the Orpheus Supersuite. Intrudes Ruth Well Formation, Karratha Granodiorite and the Andover Intrusion. Ages: 3017+/-6Ma, 3016+/-2Ma and 3014+/-2Ma. Geological province: Pilbara Craton.||||||07-FEB-11
68498|Rea Dacite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Orpheus Supersuite. Geological province: Pilbara Craton. Quartz feldspar porphyry, rhyolite and dacite; chiefly intrusive; metamorphosed.||||||07-NOV-08
68498|Rea Dacite|64580|4|Described|map legend||Mesoarchean|Of Orpheus Supersuite. Quartz-feldspar porphyritic rhyolite, and dacite; chiefly intrusive; metamorphosed.||||||15-DEC-08
68498|Rea Dacite|67201|4|Described|p16-17 Fig.9|Archean|Archean|Pilbara Craton. In Roebourne-Karratha area.||Orpheus Supersuite|||Quartz-feldspar porphyry, rhyolite, and dacite; chiefly intrusive; metamorphosed.|
68498|Rea Dacite|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Orpheus Supersuite.|||Quartz-feldspar porphyritic rhyolite, and dacite; chiefly intrusive; metamorphosed|
68498|Rea Dacite|70775|5|Briefly described|p15, p49-p50|||Pilbara Craton.|3014 +/- 2 Ma (Nelson, 1997i)|Orpheus Supersuite|||Quartz-feldspar porphyry, rhyolite and dacite, chiefly intrusive.|
68498|Rea Dacite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dacite, rhyolite|
68498|Rea Dacite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|De Grey Superbasin.|Max age 3023+/-9 Ma, min age 3014+/-2 Ma.|Orpheus Supersuite|||Rhyolite and dacite; quartz--feldspar porphyritic; chiefly intrusive; metamorphosed.|
78595|Recherche Supersuite|65487|4|Described|p,52-55, 9,13,24,27,56,58; Figs. 27, 29|Mesoproterozoic|Mesoproterozoic|Formerly the Recherche Granite. Part of the Kepa Kurl Booya Province. Intrudes Nornalup and Biranup Zones. c.1330-1280 Ma intrusion, coincides with Stage 1 of the Albany-Fraser Orogeny. Biotite-hornblende monzogranite gneiss, garnet-bearing granodiorite gneiss, and rare syn-plutonic dykes. Geochronology described in detail.|1330-1280 Ma|||||16-JAN-14
78595|Recherche Supersuite|67268|5|Briefly described|p3, p6-9, p15, p16, p19|Mesoproterozoic|Mesoproterozoic|Less abundant in the west of the Nornalup Zone. Also occurs in the Biranup Zone and Northern Foreland. Also referred to as Recherche Granite Supersuite p15/16, and Recherce Granite p16.|1289 +/- 10 Ma (U-Pb) 1302 +/- 7 Ma (SHRIMP U/Pb)|||Intrudes Dalyup Gneiss, Coramup Gneiss|Biotite-hornblende monzogranite and peraluminous garnet-bearing granodiorite gneiss. Syn-plutonic mafic dykes and aplite dykes.|15-JUN-22
78595|Recherche Supersuite|67380|5|Briefly described|p5-6, p21 Fig.15|Ectasian|Ectasian|Albany-Fraser Orogen. Uplift and erosion of this unit led to deposition of the Mount Ragged Formation.|c.1330-1280 Ma.|||||
78595|Recherche Supersuite|67722|5|Briefly described|p1, p12, 13, 14,p16, p19, p90|Mesoproterozoic|Mesoproterozoic|Nornalup Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen. Intrudes Biranup Zones and Northern Foreland. Age is of oldest felsic plutons from this supersuite.|1330 Ma-1288 Ma(SHRIMP)|||Intrudes Coramup Gneiss, Malcolm Gneiss|Granites and mafic dykes; metamorphosed to amphibolite or granulite facies; have a gneissic fabric.|
78595|Recherche Supersuite|68100|6|Mentioned|p35|Mesoproterozoic|Mesoproterozoic|See also Recherche Granite, same page.|c. 1300 Ma|||||
78595|Recherche Supersuite|68186|4|Described|p3 Fig.2, p4,p8,p11,p20-21, p26-29, p31|Mesoproterozoic|Mesoproterozoic|See also p33, p37, p40-41, p46, Plates 1A, 2. Nornalup Zone and SE Biranup Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen. Formerly the Recherche Granite. Igneous rocks are metamorphosed to amphibolite or granulite conditions. Intrusions are dated at 1330 +/- 14 Ma and 1313 +/- 16 Ma (Nelson, 1995), and described as "stitching plutons" for the converging of the combined West Australian-North Australian Craton with the combined Mawson-South Australian Craton. Ages of several other constituents are given; possible source components discussed.|1330-1283 Ma.|||Is overlain unconformably by Mount Ragged Formation. Intrudes the Malcolm Metamorphics. Is intruded by Esperance Supersuite.|Biotite-hornblende monzogranitic gneiss; peraluminous, garnet-bearing granodiorite gneiss; synplutonic mafic dykes and intrusions showing disaggregation by granite and hybrid zones of magma mingling; equigranular microgranite dykes.|
78595|Recherche Supersuite|68654|5|Briefly described|p3, p7, p15 fig 11, p16, 18, 19, 20,21|Mesoproterozoic|Mesoproterozoic|Albany-Fraser Orogen. Intrudes Biranup and Nornalup Zones of the Kepa Kurl Booya Province. Geochemical data shown and discussed.|1330-1280 Ma||||Metamonzogranites, metagranites, metasyenogranites.|
78595|Recherche Supersuite|69003|5|Briefly described|p4, p28, p39-40, p43|||Albany-Fraser Orogen. Felsic magmatic rocks. Records uplift and associated brittle deformation during the period c.1260-1225 Ma.|1330-1280 Ma.||||Strongly deformed and metamorphosed felsic plutonic rocks, with minor gabbroic rocks.|
78595|Recherche Supersuite|69140|6|Mentioned|p2-3|Ectasian|Ectasian|Geological province: Albany-Fraser Orogen.|1330-1280 Ma|||||
78595|Recherche Supersuite|69252|5|Briefly described|p5, p7 Fig.3, p9, p15-16, p20, p24, p50|Mesoproterozoic|Mesoproterozoic|See also p64, p72, p74-75, p78. Nornalup and Biranup Zones, Albany-Fraser Orogen.|1260-1215 Ma (protolith deposition age).|||Intrudes Munglinup Gneiss. Is intruded by Esperance Supersuite and Beenong Dyke Suite.|Biotite-hornblende monzogranitic gneiss with rare calc-silicate boudins, and peraluminous garnet-bearing granodiorite gneiss with no hornblende. Also mafic and aplite intrusions showing magma mixing.|
78595|Recherche Supersuite|69386|5|Briefly described|p4-6, p37|Mesoproterozoic|Mesoproterozoic|Fraser and Nornalup Zones, Albany-Fraser Orogen. Associated with an anomalous (>18.3) rare earth element index sample SE of Fraser Range homestead.|1.33-1.28 Ga.||||Deformed and recrystallised metagranite, typically amphibolite or granulite facies; has gneissic fabric and includes synmagmatic mafic rocks.|
78595|Recherche Supersuite|69595|5|Briefly described|p1, p3 fig 1, p4, p5, p14, p26, p27.|Ectasian|Ectasian|Albany-Fraser Orogen, eastern Nornalup Zone and Biranup Zone. Maximum age of this supersuite times the Stage 1 tectonic event in this area. The metasyenogranite close to the contact with the Nornalup and Biranup Zones is dated at 1317 +/- 7 Ma. The granitic gneiss at the eastern edge of the Biranup Zone was dated at 1322 +/- 11 Ma. See also p44, p45, p56.|1330 +/- 14 Ma (GSWA 83662)- c. 1280 Ma||Whalehead Rock paragneiss,||Metasyenogranite, granitic gneiss, granodioritic gneisses, syenogranitic gneisses, metagranite, metamonzogranite.|
78595|Recherche Supersuite|69729|5|Briefly described|p72-73, p88-89|Mesoproterozoic|Mesoproterozoic|Associated with Stage 1 of the Albany-Fraser Orogeny.|c.1330 Ma.||||Includes ferroan granites.|
78595|Recherche Supersuite|70023|5|Briefly described|p167-169,182,184|||Geological province: Albany-Fraser Orogen. Associated with Stage I (c. 1330-1260) Ma Albany-Fraser Orogeny, alongside voluminous felsic magmatism in Fraser Zone. Metamorphosed and deformed during Stage II (c. 1225-1140 Ma) Albany-Fraser Orogeny.|1330-1280 Ma||||Interlayered granitic and mafic gneiss.|
78595|Recherche Supersuite|70084|4|Described|p219-220,222-223,225,227-229|Ectasian|Ectasian|Geological province: Albany-Fraser Orogen, Yilgarn Craton. Associated with Stage I (1345-1260 Ma) Albany-Fraser Orogen; coeval with Fraser Range Metamorphics, and correlable to Wankanki Supersuite and Wirku Metamorphics in the western Musgrave Province. Emplaced into reworked Archean crust in a syn- to post-tectonic accretionary tectonic setting, succeeding E-dipping subduction in the Madura Province. Oldest (ca. 1330 Ma), most easterly syenogranites are adjacent Rodona Shear Zone (Albany-Fraser Orogen and Madura province boundary) and derived from melting of Madura Province crust. Limited inherited zircons in Recherche Supersuite magmas have ages of 1770-1604 Ma in keeping with a Biranup or Nornalup Zone source component.|1330-1280 Ma||Includes Fraser gabbro and GMS Suite.||Includes syenogranites, monzogranites and granodiorites.|09-JUN-20
78595|Recherche Supersuite|70085|6|Mentioned|p233|||Emplaced during the first stage of the Albany-Fraser Orogeny.|1350-1260 Ma.||||Granitic intrusions.|
78595|Recherche Supersuite|70089|6|Mentioned|p262, 264|Mesoproterozoic|Mesoproterozoic|Albany-Fraser Orogen.|1330-1280 Ma.|||||
78595|Recherche Supersuite|70090|5|Briefly described|p440-442,444-445,454,462-463|Ectasian|Ectasian|Geological province: Albany-Fraser Orogen, West Australian Craton. Felsic and mafic magmatism in the Biranup, Fraser and Normalup zones related to with Stage I (1330-1260 Ma) Albany-Fraser Orogen. Granitic gneisses are interlayered with metagabbroic sheets of Fraser Range Metamorphics. Intrudes into Snowys Dam Formation, Arid Basin.|1330-1280 Ma|||||
78595|Recherche Supersuite|70153|5|Briefly described|500k_interpgeop14_lut.csv|Mesoproterozoic|Mesoproterozoic|Another age determination is 1299 +/- 18 Ma (isotopic) - 1280 Ma (inferred).|1330 +/- 14 Ma (isotopic) - 1280 Ma (inferred).||||Granitic gneiss and metagranite; heterogeneous; locally with pods or lenses of metagabbro; may include intrusions of Esperance Supersuite. Monzogranitic gneiss; may contain remnants of Biranup Zone rocks.|
78595|Recherche Supersuite|70182|5|Briefly described|p2-6, p9-10, p13-15, p21, p33-34, p38-40|Mesoproterozoic|Mesoproterozoic|See also p43, p46-47. Stage I of the Albany-Fraser Orogeny. Geochemistry diagrams and detailed descriptions.|1330 +/- 14 Ma - 1283 +/- 7 Ma.||Gora Hill, Southern Hills, Suites.||Amphibolite or granulite facies granitic (mostly foliated metagranites or gneisses with syenogranitic, monzogranitic and granodioritic compositions) and gabbroic (generally enclaves of various sizes) intrusions.|
78595|Recherche Supersuite|70254|5|Briefly described|p357|Ectasian|Ectasian|Geological province: Nornalup Zone, Albany-Fraser Orogen. Magmatism associated with Stage I (1345-1260 Ma) Albany-Fraser Orogen.|ca. 1330-1280 Ma|||||
78595|Recherche Supersuite|70256|5|Briefly described|p2-3|Mesoproterozoic|Mesoproterozoic|Nornalup Zone, Albany-Fraser Orogen.|1330-1280 Ma.||||Voluminous granitic rocks.|
78595|Recherche Supersuite|70732|6|Mentioned|p284-285|Ectasian|Ectasian|Geological province: Albany-Fraser Orogen. Associated with Stage I (1330-1260 Ma) Albany-Fraser Orogeny.|1330-1280 Ma|||||
78595|Recherche Supersuite|70735|6|Mentioned|p28-29, 44|||Albany-Fraser Orogen.|1330-1280 Ma.|||||
78595|Recherche Supersuite|70748|6|Mentioned|p56|Ectasian|Ectasian|Albany-Fraser Orogen. SHRIMP age is derived from sample from a foliated granodiorite, 389.84-390.75m in Gambanga 1. This age is consistent with the sample being part of  the Recherche Supersuite, age range ~1330-1280 Ma.|1325 +/- 8 Ma (SHRIMP U-Pb)|||Wankanki Supersuite is broadly contemporaneous.||25-SEP-18
78595|Recherche Supersuite|70794|4|Described|2_5m_interpgeop15_lut.csv|Mesoproterozoic|Mesoproterozoic|Albany-Fraser Orogen. Also 500k_tectonicp15_lut.csv.|1330+/-14 Ma -1280 Ma|||Intruded by Esperance Supersuite.|Granitic gneiss and metagranite; heterogenous; locally with pods or lenses of metagabbro; may include intrusions of Esperance Supersuite and remnants of Paleoproterozoic basement.|
78595|Recherche Supersuite|70802|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen. Events: Albany-Fraser Orogeny Stage II (1225-1140 Ma); Albany-Fraser Orogeny (1330-1140 Ma); Albany-Fraser Orogeny Stage I (1330-1260 Ma). Typically foliated or gneissic, and metamorphosed to amphibolite or granulite facies during either Stage I or II (or both) of the Albany-Fraser Orogeny (Spaggiari et al., 2014). Sample GSWA 182462 (metagabbro) yielded a weighted mean 238U/206Pb* date of 1276+\-6 Ma, interpreted as the magmatic crystallization age of the gabbro. Sample GSWA 184125 (opx-bearing dioritic gneiss) yielded a a 207Pb*/206Pb* date of 1322+\-11 Ma, interpreted as the igneous crystallisation age of the dioritic protolith to the opx-bearing gneiss. Sample GSWA 194710 (metagranite) yielded a weighted mean 207Pb*/206Pb* date of 1317+\-7 Ma, interpreted as the magmatic crystallization age of the granite. Sample GSWA 194711 (metamonzogranite) yielded a weighted mean 207Pb*/206Pb* date of 1297+\-8 Ma, interpreted as the magmatic crystallization age of the monzogranite. Sample GSWA 194712 (metasyenogranite) yielded a concordia date of 1299+\-7 Ma, interpreted as the magmatic crystallization age of the syenogranite. Sample GSWA 194783 (metamonzogranite) yielded a concordia date of 1297+\-12 Ma, interpreted as the magmatic crystallization age of the monzogranite. See 500k_interpgeop14_lut.csv, 250k_pre_mesozoic_interpgeop_lut.csv.|1330+\14 Ma; 1299+\-18 Ma; 1280 Ma (inferred)||Includes Gora Hill Suite, Southern Hills Suite, Splinter Gneiss.||Granitic gneiss and metagranite; heterogeneous; locally with pods or lenses of metagabbro; may include intrusions of Esperance Supersuite|
78595|Recherche Supersuite|70813|5|Briefly described|p3, p5-p7, p20, p24, p26|Ectasian|Ectasian|Is the magmatic expression of Stage 1 of the Albany-Fraser Orogen. |c. 1330-1280 Ma||Includes the Southern Hills Suite and the Gora Hill Suite.||Granitic rocks.|
78595|Recherche Supersuite|70826|6|Mentioned|p10|Mesoproterozoic|Mesoproterozoic||||||Granitic rocks.|
78595|Recherche Supersuite|70831|5|Briefly described|p26|Ectasian|Ectasian|Albany-Fraser Orogen.|c. 1330-1280 Ma|||||
78595|Recherche Supersuite|71143|6|Mentioned|p442|||Geological province: Albany-Fraser Orogen.||||||
78595|Recherche Supersuite|71169|5|Briefly described|p80|Ectasian|Ectasian|Deposited during Albany Fraser Orogen, stage 1. Deposited within a convergent plate margin setting.|1330-1280 Ma||||Voluminous felsic intrusive rocks.|
78595|Recherche Supersuite|71270|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage II (1225 - 1140 Ma); Albany-Fraser Orogeny (1330 - 1140 Ma); Albany-Fraser Orogeny Stage I (1330 - 1260 Ma). See 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|1330+\-14 Ma; 1276+\-6 Ma||Includes Southern Hills Suitem Splinter Gneiss.||Granitic gneiss and metagranite; heterogeneous; locally with pods or lenses of metagabbro; may include intrusions of Esperance Supersuite and remnants of Paleoproterozoic basement|
78595|Recherche Supersuite|71488|6|Mentioned|p153|||Fraser Zone. |1330-1280 Ma|||||
78595|Recherche Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Albany-Fraser Orogen. May include intrusions of Esperance Supersuite and remnants of Paleoproterozoic basement. |max age 1330+/-14 Ma, min 1276+/-6 Ma.||Includes Splinter Gneiss, Southern Hills Suite.|May include intrusions of Esperance Supersuite. Intrudes Malcolm Metamorphics.|Granitic gneiss, metagranite; heterogeneous; locally with pods/lenses of metagabbro; may include intrusions of Esperance Supersuite + remnants of Paleoproterozoic basement. Granitic and mafic gneiss;|
78595|Recherche Supersuite|72059|5|Briefly described|p56-57,67|Ectasian|Ectasian|Geological province: Fraser Zone, Albany-Fraser Orogen. Magmatism associated with Stage I (1330-1260 Ma) Albany-Fraser Orogeny. Coeval with Wankanki Supersuite. Granitic assemblages plot mainly within the 'within plate granite field' (Kirkland et al., 2015) more typical of rift environments, where relatively dry and hot magmatism is influenced by interactions between upwelled asthenospheric magmas and crust.|1330-1280 Ma||Includes Gora Hill and Southern Hills suites.|Interleaved with Fraser Range Metamorphics.|Granitic rocks that are generally calc-alkalic.|03-FEB-20
78595|Recherche Supersuite|72710|5|Briefly described|p4 Fig.2, p8, p9 Fig.6, p19|Ectasian|Ectasian|Part of the Albany-Fraser Orogen. Includes substantial Archean inheritance.|1330 Ma to 1276 Ma.||Includes Gora Hill Suite and Southern Hills Suite||Includes granitic rocks and granitic gneisses.|
78595|Recherche Supersuite|73084|6|Mentioned|p12, p66, p122, p131-132, p139-141|Ectasian|Ectasian|Albany-Fraser Orogen.|1323 +/- 6 Ma, 1314 +/- 21 Ma, 1313 +/- 16 Ma|||Intrudes Malcolm Metamorphics|Includes granite.|
78595|Recherche Supersuite|73242|6|Mentioned|p47|||Albany-Fraser Orogen, southern.||||||
78595|Recherche Supersuite|73480|6|Mentioned|p201 Fig.1|Ectasian|Ectasian||1330-1280 Ma|||||
78595|Recherche Supersuite|73597|6|Mentioned|p1178|Mesoproterozoic|Mesoproterozoic|Nornalup Zone, Albany-Fraser Orogen.|1330-1280 Ma.||||Granite-dominated. Includes a suite of sulfide ore deposits in mafic-ultramafic intrusions.|
75278|Red Hill Granite|65264|5|Briefly described|p48 Appdx. 1|Archean|Archean|Syenogranite, porphyritic monzogranite, and granodiorite.||||||07-FEB-11
75278|Red Hill Granite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Syenogranite, porphyritic monzogranite, and granodiorite.|07-AUG-15
75278|Red Hill Granite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2662 +/- 6 Ma - 2660 +/- 10 Ma.||||Tonalite-trondhjemite; equigranular, biotite-bearing. Syenogranite, porphyritic monzogranite, and granodiorite.|
75278|Red Hill Granite|70482|5|Briefly described|p328-329|Archean|Archean|Ballarat-Last Chance deposit, Kanowna Goldfield, Eastern Goldfields Superterrane, Eastern Yilgarn Craton. Hosts the Red Hill quartz vein-hosted Au deposit. Is also referred to as Red Hill Porphyry/porphyry. Extends 1500m x 250m. Structure and mineralisation described in detail. Same ""chemical clan"" as Kanowna Belle Porphyry.||||Intrudes Kanowna Conglomerate.|A quartz albite or dacitic boss with numerous radiating dykes of similar composition.|
75278|Red Hill Granite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv, 100k_interpgeol_lut.csv.|2662+\-6 Ma; 2660+\-10 Ma||||Tonalite-trondhjemite; equigranular, biotite-bearing|
37709|Red Hill Volcanics|24140|4|Described|p214 Fig. 1|Archean|Archean|Included in  Whim Creek Group in this study based on "Copper Bore" type locality of Krapez and Eisenlohr (1998) at Red Hill.   Andesite/rhyolite. Overlies Warambie Basalt. Age: c.3009+/-4Ma (Nelson 1998).||||||07-NOV-08
37709|Red Hill Volcanics|24191|4|Described|p829, p830 Fig. 2|Archean|Archean|Of Whim Creek Group.  Overlies Warambie Basalt.  Intruded by Mons Cupri Dacite.  Together with Mons Cupri Dacite, supersedes Mons Cupri Volcanics.  Geological Province: Pilbara Craton.||||||07-NOV-08
37709|Red Hill Volcanics|24550|5|Briefly described|p36 Tb. 3.2|Archean|Archean|Of the Whim Creek Group. Dominated by andesite and rhyodacite, with sandstone and breccia. Overlie Warrambie Basalt. Intruded by Mons Cupri Dacite. Age: ca 3010Ma. Thickness: 300m. Geological Province: Pilbara Craton.||||||07-FEB-11
37709|Red Hill Volcanics|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Age: <3.0Ga. Geological Province: Pilbara Craton.||||||07-NOV-08
37709|Red Hill Volcanics|63441|5|Briefly described|p5 Tb.1|Archean|Archean|Of Whim Creek Group (Pilbara Supergroup). Contains the Mons Cupri Dacite Member and together these two supersede Mons Cupri Volcanics. Geological province: Whim Creek Basin, Pilbara Craton.||||||07-FEB-11
37709|Red Hill Volcanics|63538|4|Described|p6 Fig. 3|Archean|Archean|Of Whim Creek Group. Underlain by Warambie Basalt. Geological Province: Pilbara Craton. Felsic volcanic rocks.||||||19-APR-13
37709|Red Hill Volcanics|64174|5|Briefly described|Map legend|Archean|Archean|Of Whim Creek Group (De Grey Supergroup).  Age: <3016-3009Ma. Geolprov: Whim Creek Basin, Pilbara Craton. Felsic volcaniclastic rocks, intrusive porphyritic dacite+dacitic to rhyolitic lava; includes debris-flow, turbidite + fluvial facies; metamorphosed.||||||07-NOV-08
37709|Red Hill Volcanics|64580|4|Described|map legend||Mesoarchean|Of Whim Creek Group. Felsic volcaniclastic rocks, intrusive porphyritic dacite and dacitic to rhyolitic lava; includes debris-flow, turbidite and fluvial facies; metamorphosed.||||||15-DEC-08
37709|Red Hill Volcanics|66217|5|Briefly described|p39.|Mesoarchean|Mesoarchean|Whim Creek Basin.|3009 +/- 4 Ma (Nelson 1998f).|Unit in Whim Creek Group.||||
37709|Red Hill Volcanics|67201|4|Described|p7, p12, p16-17, p21, p23, p64-67|Archean|Archean|In northwestern Pilbara Craton, West Pilbara Superterrane, De Grey Superbasin, Whim Creek Basin. c. 3000-2990 Ma includes Pb-Pb ages between 3150-2995 Ma confirming detrital component.|3009+/-4 Ma breccia (U-Pb SHRIMP Nelson 1998)|Whim Creek Group|||Felsic volcaniclastic rocks, intrusive porphyritic dacite and dacitic to rhyolitic lava, basaltic breccia; tabular bedded sandstone and siltstone facies; includes debris-flow, turbidite and fluvial facies; metamorphosed.|25-NOV-16
37709|Red Hill Volcanics|69185|5|Briefly described|500k_geologyp08_lut.csv||Mesoarchean|||Unit of Whim Creek Group.|||Felsic volcaniclastic rocks, intrusive porphyritic dacite and dacitic to rhyolitic lava; includes debris-flow, turbidite and fluvial facies; metamorphosed|
37709|Red Hill Volcanics|69299|5|Briefly described|p6 Tb.1|||Thickness on COOYA POOYA: 0-500 m.|c. 3009 Ma|Of Whim Creek Group. |||Felsic volcanic and volcaniclastic rocks, and dacite intrusions.|01-JUL-14
37709|Red Hill Volcanics|69300|5|Briefly described|map legend|Archean|Archean|Whim Creek Basin (and Mallina Basin?), Whim Creek greenstone belt||Whim Creek Group||||
37709|Red Hill Volcanics|69301|4|Described|p5 Fig.3, p9 Tb.1, p15|||Pilbara Craton. West Pilbara Superterrane. Whim Creek Basin.|3000 Ma|Whim Creek Group|||Felsic volcanic rocks.|
37709|Red Hill Volcanics|69590|4|Described|500k_geologyp08_lut.csv||Mesoarchean|||Unit of Whim Creek Group.|||Felsic volcaniclastic rocks, intrusive porphyritic dacite and dacitic to rhyolitic lava; includes debris-flow, turbidite and fluvial facies; metamorphosed|
37709|Red Hill Volcanics|70022|6|Mentioned|p115|||West Pilbara Superterrane.||Whim Creek Group.||||
37709|Red Hill Volcanics|70775|4|Described|p12, p15, p18, p29|Mesoarchean|Mesoarchean|Whim Creek Basin. Contains inherited zircon dated at 3154 +/- 8 Ma and 3141 +/- 5 Ma. Previously the Mons Cupri Volcanics before being renamed by Pike et al., 2002. See also p41, p43-p46, p50-p53, p60, p62, p75, p81.|c. 3009-2991 Ma|Whim Creek Group|Includes the Mons Cupri Dacite Member.|Overlies the Warambie Basalt. Unconformably overlain by the Cistern Formation. Intruded by the Mons Cupri Dacite Member.|Felsic volcaniclastic rocks, intrusive porphyritic dacite and dacitic to rhyolitic lava; includes debris flow, turbidite and fluvial facies; metamorphosed.|
37709|Red Hill Volcanics|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Whim Creek Basin.|Max age 3009+/-4 Ma, min 2991+/-12 Ma.|Whim Creek Group|||Felsic volcaniclastic rocks, intrusive porphyritic dacite and dacitic to rhyolitic lava; includes debris-flow, turbidite and fluvial facies; metamorphosed.|
37709|Red Hill Volcanics|72251|5|Briefly described|p54|Mesoarchean|Mesoarchean|Geological province: West Pilbara Superterrane, Pilbara Craton.||Unit of Whim Creek Group.||Overlain unconformably by Cistern Formation. Underlain by Warambier Basalt. Correlable to Constantine Sandstone.||
37709|Red Hill Volcanics|72668|5|Briefly described|p4, p14|||West Pilbara Superterrane.||Whim Creek Group|Includes the Mons Cupri Dacite Member.|Overlies the Warambie Basalt.|Rhyodacite to dacite.|
31894|Red Rock Formation|22440|6|Mentioned|p4|||||||||
31894|Red Rock Formation|22547|5|Briefly described|p14||Orosirian|c. 1800. Overlain by Texas Downs Formation||||||
31894|Red Rock Formation|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
31894|Red Rock Formation|22754|5|Briefly described|p10 Tb. 2, p5 Tb. 1|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
31894|Red Rock Formation|23621|5|Briefly described|p22|||||||||
31894|Red Rock Formation|24173|6|Mentioned|p22|||Unconformably overlies McHale Granodiorite. Equivalent on the McINTOSH and TURKEY CREEK maps to outcrops shown as Kimberley Group east of Mount Barret but considered as a separate unit.||||||06-APR-05
31894|Red Rock Formation|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Sandstone, feldspathic sandstone, pebbly sandstone, conglomerate, siltstone, mudstone, basalt and basaltic breccia.  Geological Province: Red Rock basin.||||||07-NOV-08
31894|Red Rock Formation|43854|5|Briefly described|Map Legend||Proterozoic|||||||
31894|Red Rock Formation|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31894|Red Rock Formation|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Red Rock Basin. Fine to coarse grained lithic quartz sandstone, pebbly sandstone, conglomerate, siltstone, mudstone, basalt flows and basaltic breccia. Carbonate rock.||||||
31894|Red Rock Formation|60533|5|Briefly described|p604|||Unconformably overlies: Tickalara Metamorphics and McHale Granite. ||||||
31894|Red Rock Formation|63866|5|Briefly described|p132|||||||Unconformably overlies the McHale Granodiorite. Possibly equivalent to the Kimberley Group.||
31894|Red Rock Formation|64580|4|Described|map legend||Paleoproterozoic|Sandstone, feldspathic sandstone, pebbly sandstone, conglomerate, siltstone, mudstone, basalt and basaltic breccia.||||||15-DEC-08
31894|Red Rock Formation|65413|5|Briefly described|p104, p106 Fig.2.|Paleoproterozoic|Paleoproterozoic|||||Unconformably overlies McHale Granodiorite. Is faulted against Helicopter Siltstone.||20-FEB-17
31894|Red Rock Formation|67127|5|Briefly described|p113, p174|Proterozoic|Proterozoic|Hosts REE mineralisation near the western end of the Osmond Range, East Kimberley.|||||Lithic quartz sandstone and conglomerate.|
31894|Red Rock Formation|68078|6|Mentioned|p23|||Broadly similar to lower Kimberley Group, may be broadly coeval.||||||
31894|Red Rock Formation|69003|6|Mentioned|p5, p19|||Lamboo Province, Halls Creek Orogen.||||||
31894|Red Rock Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Red Rock Basin|||Includes 3 unnamed members.||Lithic quartz sandstone, pink feldspathic quartz sandstone, pebbly sandstone, conglomerate, siltstone, mudstone, massive to amygdaloidal basalt flows, and basaltic breccia, dolerite; carbonate rock|04-AUG-15
31894|Red Rock Formation|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv. |||||Lithic quartz sandstone, pink feldspathic quartz sandstone, pebbly sandstone, conglomerate, siltstone, mudstone, basalt flows and breccia. Carbonate rock, dolerite and amygdaloidal basalt.|
31894|Red Rock Formation|69585|6|Mentioned|p4-5|Statherian|Statherian|Lamboo Province.||||Probable equivalent of the Kimberley Group.||
31894|Red Rock Formation|69597|6|Mentioned|p5 fig 2b|||||||||
31894|Red Rock Formation|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Red Rock Basin. Events: King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1. See 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|1827-1784 Ma (Inferred)||||Lithic quartz sandstone, pink feldspathic quartz sandstone, pebbly sandstone, conglomerate, siltstone, mudstone, massive to amygdaloidal basalt flows and basaltic breccia, and dolerite; minor lithic sandstone, siltstone, and mudstone, carbonates|
31894|Red Rock Formation|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv.|1784-1827 Ma||||Lithic quartz sandstone, pink feldspathic quartz sandstone, pebbly sandstone, conglomerate, siltstone, mudstone and basalt and basaltic breccia, Carbonate rock.|
31894|Red Rock Formation|70731|6|Mentioned|p268,272-273|Stathetian|Stathetian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.||||||
31894|Red Rock Formation|70812|5|Briefly described|p6, p29|Statherian|Orosirian|Central and Eastern zones of the Halls Creek Orogen, Lamboo Province.|c. 1800-1750 Ma|||||
31894|Red Rock Formation|70851|5|Briefly described|p4, p11-p12|Paleoproterozoic|Paleoproterozoic|Central and Eastern zones, Lamboo Province. Rock properties are provided.|c. 1800-1750 Ma|||||
31894|Red Rock Formation|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Red Rock Basin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|1827-1784 Ma (inferred)||||Lithic quartz sandstone, pink feldspathic quartz sandstone, pebbly sandstone, conglomerate, siltstone, mudstone, massive to amygdaloidal basalt flows and basaltic breccia, and dolerite; minor lithic sandstone, siltstone, and mudstone, carbonate rock|
31894|Red Rock Formation|71397|6|Mentioned|p5|Proterozoic|Proterozoic|Geological province: Central and Eastern zones, Lamboo Province, Halls Creek Orogen.||||||
31894|Red Rock Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Red Rock Basin.|||||Lithic quartz sandstone, pink feldspathic quartz sandstone, pebbly sandstone, conglomerate, siltstone, mudstone, basalt flows, and basaltic breccia.|
36777|Red Rock Granite|24183|6|Mentioned|p7|||||||||
77942|Redeemer Basalt|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2720 - 2680 Ma (inferred).|Two Sisters Subgroup|||Basalt; locally pillowed; metamorphosed.|
77942|Redeemer Basalt|70326|3|Fully described|p334,336,338,341-2,349-51,353-7,360-1|Neoarchean|Neoarchean|Geological province: Agnew region, Ora Banda Domain, Kalgoorlie Terrane, Yilgarn Craton. Subaqueous extrusive basalts (komatiitic basalt) intruded by a more evolved comagmatic (high-Mg tholeiite) sill. Contemporaneous to, and interdigitates with Burrell Well Basalt. Thickness: 100-405m thick; fine-grained basic 70-280m; coarse-grained basic-ultrabasic 30-125m. Observed in many drillholes on western limb of Agnew Anticline and in outcrop in the Mount White Syncline. Major and trace element geochemical analysis on Table 4 p342-346. Evidence of crustal contamination e.g. negative Nb and T ianomalies; [La/Sm]PM> 1; Pearce, 2008; van Hunen and Moyen, 2012). TIMS U-Pb crystallisation age of comagmatic intrusion interpreted to be 2686.8+\-3.0 Ma. See also p363-4.||||Overlain by White Hope Basalt. Interdigitates with Burrell Well Basalt. Correlable to Bent Tree and Gleesons basalts.|Fine-grained basic (pillow, sheet flows), coarse-grained basic-ultrabasic (sub-volcanic intrusions). Basalt: texturally indistinguishable from Burrell Well Basalt. Includes 2 thin mudstones, and submarine pillow, sheet flows, comagmatic intrusions.|03-SEP-19
77942|Redeemer Basalt|71212|5|Briefly described|intro p2|||Yilgarn Craton. ||Two Sisters Subgroup||||
77942|Redeemer Basalt|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2711-2687 Ma (inferred)|Unit of Two Sisters Subgroup.|||Basalt; locally pillowed; metamorphosed|
77942|Redeemer Basalt|73151|5|Briefly described|p3, p5, p10, p12-13, p16|Neoarchean|Neoarchean|Yilgarn Craton. Kalgoorlie Terrane, Agnew Greenstone Belt.||Kalgoorlie Group||Overlies Burrell Well Basalt, underlies White Hope Basalt, unconformably underlies Scotty Creek Formation.|Massive basalt.|
77942|Redeemer Basalt|73596|6|Mentioned|p1152, 1157-1158, 1160, 1162, 1167|Neoarchean|Neoarchean|Agnew-Wiluna Greenstone Belt. Deep-water mafic-ultramafic lava fields and feeder intrusions.||Two Sisters Subgroup.||Overlies Burrell Well Basalt and Agnew Komatiite. Is overlain by White Hope Basalt.||
34564|Redgate Coal Measures|12758|4|Described|p14, p3 Fig. 3|Late Permian - Correct|Late Permian - Correct|Of the Sue Group.  Predominantly sandstone with intercalations of siltstone, shale and thin coal seams.  Conformably overlain by Willespie Fm; conformably overlies Ashbrook Sandstone.  Max. thickness: 165m.  Geol.Prov: Perth Basin. See also p8 Fig. 9.||||||
34564|Redgate Coal Measures|14227|5|Briefly described|Enclos. 2|Artinskian|Artinskian|Of the Sue Group. Overlies Ashbrook Coal Measures; underlies Willespie Formation. Geol. Prov: Bunbury Trough, southern Perth Basin.||||||07-FEB-11
34564|Redgate Coal Measures|22818|5|Briefly described|map|Late Permian|Late Permian|Sue Group||||||
34564|Redgate Coal Measures|22819|5|Briefly described|map|Late Permian|Late Permian|Sue Group||||||
34564|Redgate Coal Measures|22820|2|Defined|p8 Tb. 1, p19|Late Permian|Late Permian|Of Sue Group.Conformable on Ashbrook Sandst; conformable below Willespie Formation. Max. thickness: 300m. Geol.prov: S. Perth Basin. Predom'ly sandstone, intercalated with sst/siltst. units, argillaceous units + many thin coal seams; alluvial fan deposits||||||12-AUG-08
34564|Redgate Coal Measures|24443|5|Briefly described|Fig.31|Late Permian|Late Permian|Of Sue Group. Conformably overlies Ashbrook Sandstone. Conformably overlain by Willespie Formation. Geological Province: Perth Basin.||||||
34564|Redgate Coal Measures|50107|5|Briefly described|Map legend|Permian|Permian|Of the Sue Group.  Geological Province: Southern Perth Basin.||||||
34564|Redgate Coal Measures|60386|5|Briefly described|p296, 311|Cisuralian|Cisuralian|Southern Perth Basin. Shown as Early Permian. Non-marine.||||||
34564|Redgate Coal Measures|64630|5|Briefly described|p31 Fig.2|Roadian|Artinskian|Province: Southern Perth Basin. Overlies the Ashbrook Sandstone, underlies the Willespe Formation. Palynology age: M. trisina to D. granulata. Middle correlates with Allandale Sandstone.||||||23-JUL-15
34564|Redgate Coal Measures|67925|4|Described|Ch2 p10 fig 4, Ch2 p11-p12|Kazanian|Ufimian|A type section in the Sue1 drillhole is described as being 146m thick. Interpreted to have been deposited in an alluvial environment that ranged from braided streams to swamp and lacustrine deltas. Palynology discussed. Incorrectly referred to informally as the Redgate coal measures in Ch2 p15. See also Ch2 p15, Ch2 p28, Ch2 p30, Ch2 p44-p45, Ch3 p8, Ch4 p8 fig 2.||Sue Group||Overlies the Ashbrook Sandstone. Conformably overlain by the Willespie Formation.|Coaly, poorly sorted feldspathic sandstone.|
34564|Redgate Coal Measures|69029|6|Mentioned|p332|Wordian|Roadian|Of Perth Basin.||||||
34564|Redgate Coal Measures|69081|5|Briefly described|p737 Fig.1|Guadalupian|Guadalupian|Presented as Redgate Coal Ms in figure. Geol. Prov: Perth Basin.||Sue Group||Is overlain by Willespie Formation; overlies Ashbrook Sandstone.||23-JUL-15
34564|Redgate Coal Measures|69182|6|Mentioned|Ch2 p9, Ch2 p45, Ch2 p47-p49|Early Permian|Early Permian|Perth Basin. See also Ch2 p55, Ch2 p57, Ch2 p60, Ch2 p64-p66, Ch2 p80, Ch2 p84, Ch2 p91, Ch2 p92, Ch2 p94-p96, Ch2 p98, Ch2 p100, Ch2 p102, Ch2 p104, Ch2 p106, Ch2 p108, Ch2 p110.||Sue Group||Overlies the Ashbrook Sandstone. Overlain by the Willespie Formation.||
34564|Redgate Coal Measures|69297|6|Mentioned|p175, p187, p189|Wordian|Roadian|Vlaming Sub-basin, South Perth Basin. ||Sue Group||Overlies the Ashbrook Sandstone. Overlain by the Willespie Formation.||
34564|Redgate Coal Measures|70097|5|Briefly described|p2, p19 Fig.3|Wordian|Kungurian|Southern Perth Basin. Bunbury Trough.||Sue Group||Overlies Ashbrook Sandstone. Is overlain by Willespie Formation.|Deglaciation, deltaic sediments. Includes coal.|12-SEP-17
34564|Redgate Coal Measures|70099|5|Briefly described|Fig.4|Wordian|Kungurian|||Sue Group.||Overlies Ashbrook Sandstone. Is overlain by Willespie Formation.||
34564|Redgate Coal Measures|70128|5|Briefly described|p449|Permian|Permian|Southern Perth Basin.||Sue Group.||Conformably overlies Ashbrook Sandstone. Is overlain conformably by Willespie Formation.||
34564|Redgate Coal Measures|70774|5|Briefly described|p5 fig 3|Ufimian|Artinskian|Southern Perth Basin.||||Overlies the Ashbrook Sandstone. Unconformably? Overlain by the Willespie Formation.||
34564|Redgate Coal Measures|71146|5|Briefly described|p6,  p43 fig 33|Guadalupian|Guadalupian|Perth Basin.||||Overlies the Ashbrook Sandstone. Overlian by the Willespie Formation.|Mixed sandstone, mudstone and coal.|
34564|Redgate Coal Measures|71377|5|Briefly described|p7|Permian|Permian|Perth Basin.||Stockton Group||||
34564|Redgate Coal Measures|71958|5|Briefly described|p34|Wordian|Roadian|Vlaming Sub-basin.||Sue Group||Overlies the Ashbrook Coal Measures. Overlain by the Willespie Formation.||
34564|Redgate Coal Measures|72258|5|Briefly described|p129|Guadalupian|Cisuralian|Of Perth Basin.||||Overlain by Willespie Formation. Underlain by Ashbrook Sandstone. Laterally grades into Irwin River Coal Measures.||
22744|Redmine Group|23584|5|Briefly described|p31 Fig 17|Holocene|Oligocene|Underlying unit Eundynie Group.||||||
22744|Redmine Group|23797|5|Briefly described|p3|Tertiary|Tertiary|Includes Cowan Dolomite. Age: Late Tertiary. Overlies Norseman Limestone. Geological Province: Yilgarn Craton.||||||15-AUG-06
22744|Redmine Group|42959|5|Briefly described|p58 Fig.3|||||||||
22744|Redmine Group|43761|6|Mentioned|p420|||||||||
22744|Redmine Group|43838|5|Briefly described|p4||Tertiary|Contains Cowan Dolomite, Beta Island Member, Roysalt Formation & Polar Bear Formation. Lacustrine.||||||12-JUL-16
22744|Redmine Group|64340|6|Mentioned|p26 Tb. 5, p26|Holocene|Oligocene|||||||
22744|Redmine Group|65260|6|Mentioned|p27 Fig.20|Holocene|Oligocene|Overlies Eundynie Group.||||||
22744|Redmine Group|69152|5|Briefly described|1m_geologyp08_lut.csv|Eocene|Eocene||||Includes Cowan Dolomite.|||
22744|Redmine Group|69598|6|Mentioned|p2, p9, p10, p11 Tb.1, p29 Tb.4|Holocene |Oligocene|Eucla Basin. Up to 40m thick. |||Includes the Revenge Formation, Gamma Island Formation, the Roysalt Formation, the Polar Bear Formation and the Cowan Dolomite.|||
22744|Redmine Group|71270|5|Briefly described|1m_geologyp12_lut.csv|||Geological province: Yilgarn Craton, West Australian Craton. |||Includes Cowan Dolomite.|||
74820|Reedy Trondhjemite|64891|5|Briefly described|p42, p50-51 Tb. 1|Archean|Archean|Of Cullculli Suite (Annean Supersuite). Age: 2785+/-8Ma. Geological province: Murchison Domain. Trondhjemite; metamorphosed.||||||07-FEB-11
74820|Reedy Trondhjemite|69583|5|Briefly described|p49|Neoarchean|Neoarchean|Murchison Domain.||Cullculli Suite.||||
74820|Reedy Trondhjemite|69584|5|Briefly described|p5 Fig.2|Neoarchean|Neoarchean|||CullCulli Suite|||Trondhjemite.|
74820|Reedy Trondhjemite|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Cullculli Suite.||||
32171|Reeves Formation|23523|4|Described|p989|Carboniferous|Carboniferous|See also p 997. Geological Province: Canning Basin.||||||
32171|Reeves Formation|24466|5|Briefly described|p365|Carboniferous|Carboniferous|Formerly referred to as the Lower Grant Group.||||||
32171|Reeves Formation|60386|6|Mentioned|p297|Carboniferous||Roebuck/Canning Basin. Deltaic - nearshore - shelf. ||||||
32171|Reeves Formation|61021|5|Briefly described|p36 Fig. 2|Asselian|Namurian|Geological Province: Canning Basin.||||||17-DEC-07
32171|Reeves Formation|64630|5|Briefly described|p31 Fig.2, p35, 37|Asseliean|Bashkirian|N.B. Formerly the Betty Formation of the Grant Group. Tentative dates. Province: Canning Basin. Part of the Grant Group, underlies the Winifred Formation. Palynology age: S. ybertii to at least D. tenuistriatus. Inferred glacial influence.||||||11-JAN-10
32171|Reeves Formation|64643|5|Briefly described|p3 Fig. 2, p21|Pennsylvanian|Pennsylvanian|Disconformably overlain by Grant Group in Fitzroy Trough.||||||24-NOV-08
32171|Reeves Formation|64971|2|Defined|p683-688, including p685 Fig. 2|Visean|Early Permian|New stratigraphic unit includes most of the interval previously assigned to loosely defined Grant Group, Lower. Overlain by revised Grant Gp (this paper) in Fitzroy Trough, underlain unconformably by Anderson Fm. Thick: 1255m. Sandstone.||||||10-APR-13
32171|Reeves Formation|64972|6|Mentioned|p615|||Geological Province: Canning Basin.||||||
32171|Reeves Formation|65301|5|Briefly described|p5 Fig. 4, p8 Fig. 5|Pennsylvanian|Pennsylvanian|Geological province: Canning Basin.||||||
32171|Reeves Formation|65382|5|Briefly described|p714, p717 App. 2|Stephanian|Visean|Canning Basin. Formerly 'Lower Grant'.  Age of </= 327 Ma given. Glaciomarine. Includes palynofloras indicating late Visean to Stephanian age. Correlated in part with Lake Galilee Sandstone.||||||07-MAR-12
32171|Reeves Formation|65449|6|Mentioned|p6|Late Carboniferous|Late Carboniferous|||||Unconformably overlies Anderson Formation. Is overlain unconformably by Grant Group.||
32171|Reeves Formation|66949|4|Described|p58 App.3, p1, p3, p4 Fig.2, p5, p7-11,|Gzhelian|Serpukhovian|See also  p13, p16, p18, p28, p31; p46-48,50-54 Appx.2, , p60-65 Appx.4, p66-84,86-94 Appx.5; p119-120 Appx.7; Plates 2-12. Basal glacial succession in Canning Basin. Formerly much of the Betty Formation of the Grant Group; excluded from Grant Group by Apak and Backhouse (1998, 1999). Type section detailed (and modified in this study). Age from palynology. Up to 2000m thick; glacial deltaic to fluvial deposits. Biostratigraphy: brief discussion of inclusion of the Grandispora maculosa zone (Kemp, 1977). Reservoir and oil source properties discussed. Available core and Formation picks detailed. TOC and Rock-Eval data.||||Overlies Anderson Formation ?unconformably. Is overlain by Grant Group.|Sandstone, mudstone and diamictite.|30-OCT-15
32171|Reeves Formation|67354|5|Briefly described|p107.|Late Carboniferous|Late Carboniferous|Crossland Platform. May contain incised tunnel valleys.||||||
32171|Reeves Formation|67888|6|Mentioned|p42|Triassic|Carboniferous|Good oil reservoir potential identified.||||||
32171|Reeves Formation|68007|5|Briefly described|p2, p4, Plate 1|Late Carboniferous|Carboniferous|Kidson Sub-basin.||||Unconformably overlies Clapp Ridge Formation. Is overlain by Grant Group.||26-FEB-20
32171|Reeves Formation|68902|6|Mentioned|p9 fig 5|Carboniferous|Carboniferous|||||Unconformably overlies Anderson Formation. Is overlain unconformably (locally conformably) by Grant Group.||
32171|Reeves Formation|69029|6|Mentioned|p319|Gzhelian|Serphukovian|Of Canning Basin.||||Overlain by Grant Group. Underlain by Anderson Formation.||
32171|Reeves Formation|69182|6|Mentioned|Ch4 p9, Ch4 p13-p14, Ch4 p38|Pennsylvanian|Serpukhovian|North Canning Basin. See also Ch4 p39, Ch4 p42, Ch4 p44, Ch4 p45, Ch4 p47, Ch4 p50-p58, Ch4 p63-p65, Ch4 p74-p77, Ch4 p84, Ch4 p88, Ch4 p90, Ch4 p96.||||Overlain by the Grant Group. Unconformably overlies the Anderson Formation.||
32171|Reeves Formation|69297|6|Mentioned|p337, p352, p355|Gzhelian|Moscovian|Broome Platform of the Canning Basin. ||Grant Group||Unconformably overlies the Laurel Formation of the Fairfield Group. Overlain by the Hoya Formation.||
32171|Reeves Formation|69312|6|Mentioned|p3, p7, p19, p23 fig 27|Gzhelian|Serpukhovian|Canning Basin. See also p24 fig 29, p25 fig 31, p26 fig 33, p28 fig 35, p29 fig 37. ||||Faulted against the Anderson Formation [?].. Overlain by the Grant Group.|Sandstone and shale.|11-FEB-20
32171|Reeves Formation|69693|5|Briefly described|p3|Gzhelian|Serpukhovian|Mory (2010). Canning Basin. See also references to Reeves formation (p4).||||Unconformably overlies Anderson Formation. Is overlain unconformably by Grant Group.||
32171|Reeves Formation|70492|6|Mentioned|p166|Late Carboniferous|Early Carboniferous|Fitzroy Trough, Canning Basin.||||Is overlain by Grant Group.||
32171|Reeves Formation|70774|5|Briefly described|p4, p9|Pennsylvanian|Mississippian|Fitzroy Trough, Lennard Shelf and Willara and Kidson Sub-basins, Canning Basin.||||Unconformably overlies the Anderson Formation. Overlain by the Grant Group.||
32171|Reeves Formation|71146|5|Briefly described|p6,  p43 fig 33|Moscovian|Serpukhovian|Canning Basin.||||Unconformably overlies the Anderson Formation. Unconformably overlain by the Grant Group.|Sandstone.|
32171|Reeves Formation|71870|5|Briefly described|p3|Gzhelian|Serpukhovian|Canning Basin.||||Overlies the Anderson Formation. Unconformably overlain by the Grant Group.||
32171|Reeves Formation|71894|5|Briefly described|p3-p4, p20, p27|Pennsylvanian|Serpukhovian|Canning Basin. Laterally extensive across the basin.||||Unconformably overlies the Anderson Formation. Unconformably overlain by the Grant Group.|Sandstone and diamictite.|
32171|Reeves Formation|72496|4|Described|p217-227, p229-231|Asselian|Serpukhovian|Canning Basin, Fitzroy Trough, absent on the Lennard Shelf and Barbwire Terrace. Initially termed the Lower Grant Group (Redfern, 1990; O'Brien et al., 1998) but was redefined by Apak and Backhouse (1999). Interpreted to have been deposited during the Late Carboniferous Point Moody Extension phase as a syn-rift sequence. Thickness ranges from 71.5m in wells to in excess of 1875m; the maximum drilled thickness is 1241.8 m in Nerrima AFO-1. Characterised by medium-amplitude seismic reflection.||||Unconformably overlain by the Grant Group. Overlies the Anderson Formation. Unconformably overlain by the Betty Formation.|Dominantly sandstone with some diamictite and mudstone..|18-MAR-20
32171|Reeves Formation|72499|4|Described|p6, p7, p8, p11, p20, p22, p24, p25, 54|Pennsylvanian|Serpukhovian|Previously 'Lower Grant Group'. Identified in well logs Sundown 1 (Lennard Shelf) and The Sisters 1 and Scarpia 1 (Fitzroy Trough). Located in the Fitzroy Trough.||||Shown as unconformably overlying Anderson Formation and underlies Grant Group.|Includes sandstone, shale, glacigenic sediments and diamictite.|
32171|Reeves Formation|72504|5|Briefly described|Figure 1-2|Moscovian|Visean|Canning Basin.Interpreted to have a restricted distribution entirely in the northern Canning Basin on the basis of new biostratigraphic correlation. Maximum known thickness is 715m in Grant Range 1 hole. Thins to the north and the south as a result of basal onlap, erosion or nondeposition. Dominantly fluvial in origin. Biostratigraphy is discussed.||||||
32171|Reeves Formation|73117|3|Fully described|[See comments].|Moscovian|Visean|Canning Basin; Fitzroy Trough, Gregory Sub-basin and adjoining sub-basins to the north. Restricted to the subsurface in the northwest. Type section: 922.3 - 1410.2 m in Fraser River 1 [revised here]. Fluvial facies up to 700 m thick [also written as siliciclastic facies up to 715 m thick]. Equivalent to glacial strata in other parts of Gondwana, but doesn't show obvious glacial characteristics. Contain possible diamictitic facies but does not support an unambiguous glacial origin; although, this may be a function of how little core exists for this unit (115 m of mostly degraded core from seven wells). Interpreted as deposited by a sand-dominated, low-sinuosity, fluvial system with no sign of glacial influence; minor marine influence is indicated by macrofossils (bivalves and a brachiopod). Lacks bioturbation and exotic clasts and grains. Significant basal unconformity representative of Meda Transpression. No lithostratigraphic regional marker horizons / significant [lateral] facies changes. Previously included as the lower portion of the Grant Formation [now Grant Group] and distinguishing between the two is highly reliant on palynozonation. No wells south of the Fitzroy Trough have unambiguous palynozonation determinations to support identification of this unit. Can also be difficult to differentiate from the Anderson Formation in the absence of biostratigraphic data. Includes Grandispora maculosa, Spelaeotriletes ybertii and Diatomozonotriletes birkheadensis Zones [palynology], which have highly variable thickness. [Article includes detailed palynomorph biostratigraphy]. Thermal maturity data indicate deeper parts may be/have been within the oil window. Other data indicates low-generating potential but may be suitable for reservoir-seal couplets including [sandstones] with up to 25% porosity and mudstones that can form effective top seals.  p: 1-5, 10, 12-17, 19-25, 31-34, 36-39, 54-56, 58, 62, 70, 72, 109-111, 113-132, 135-140, 142.||||Unconformably underlain by Laurel Formation and Anderson Formation. Unconformably overlain by Grant Group. Approximately coeval with Wadeye Group.|Dominantly sandstone with minor mudstone.|
32171|Reeves Formation|73184|5|Briefly described|p184, p187 Fig.3, p188, p200-201|Moscovian|late Visean|Canning Basin. Predominantly a syn-rift, fluvial-dominated and pre-glacial succession. Significant expansion of the Reeves Formation towards the southern major basin bounding faults. Late Visean to ca. Moscovian age in the Fitzroy Trough based on palynology. No direct evidence for glaciation. Probable depositional hiatus and/or erosion spanning at least from the middle to late Pennsylvanian between the Reeves Formation and Grant Group in the Fitzroy Trough, larger break on the flanking sub-basins.||||Underlies the Grant Group.|Predominantly composed of homogeneous sandstone with minor intervening silt and mudstone.|
32171|Reeves Formation|73345|6|Mentioned|p230|||Canning Basin. Not present in Barnicarndy 1 well based on palynology results, primarily of Grant Group samples.||||Overlain by Grant Group.||
28962|Revels Corner Sandstone Member|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Irregully Formation.||||||
28962|Revels Corner Sandstone Member|34066|4|Described|p11|||||||||
28962|Revels Corner Sandstone Member|36884|4|Described|p153|||||||||
28962|Revels Corner Sandstone Member|40089|4|Described|p24|||||||||
28962|Revels Corner Sandstone Member|44481|5|Briefly described|map legend||Mesoproterozoic|Part of Irregully Formation.||||||
28962|Revels Corner Sandstone Member|72758|5|Briefly described|p8 Tb.1, p50, p53.|||c. 330 m thick. Part of the 2800m thick Irregully Formation. Not recognized south of the Ashburton River. Incorrectly termed Revels Corner Dolomite Member in contents (p iv).||Irregully Formation||Conformably overlies Warrada Dolomite Member.|Brown-weathering, thin-bedded sandstone, some of which contain mudstone clasts.|
22753|Revenge Formation|14227|5|Briefly described|Enclos. 2|Early Miocene|Early Oligocene|Presented as Revenge FM + Cowan Dolomite.||||||07-FEB-11
22753|Revenge Formation|23138|5|Briefly described|p240|Miocene|Oligocene|||||||
22753|Revenge Formation|23989|5|Briefly described|p54|Cenozoic|Cenozoic|See also page 54 Fig.46. Geological Province: Yilgarn Craton||||||19-NOV-08
22753|Revenge Formation|42959|5|Briefly described|p62|||see also p58 Fig 3||||||
22753|Revenge Formation|43761|5|Briefly described|p420-421||Miocene|||||||
22753|Revenge Formation|61155|5|Briefly described|p17|Late Miocene|Late Oligocene|Over and under and interfingers with Gamma Formation. Age: ~29-10.5Ma. Thickness: 25m. Geological region: Norseman region. ||||||
22753|Revenge Formation|64646|6|Mentioned|p23 Fig. 3, p24 Fig. 4|Miocene|Oligocene|Geological Province: Yilgarn Craton.||||||08-FEB-10
22753|Revenge Formation|65194|5|Briefly described|p135, p136 Fig.4.37|||Post-Eocene sediments in Cowan and parts of Lefroy Palaeovalleys. Oxidised non-marine, fine-grained clastic deposits.||||||
22753|Revenge Formation|69598|5|Briefly described|p2, p9, p10, p11 Tb.1, p29 Tb.4|Middle Miocene|Late Oligocene|Eucla Basin. Contains potential sealing lithologies. ||Redmine Group|||Siltstones and sideritic claystones.|
34206|Rhodda beds|22649|5|Briefly described|p 151|||Province - Officer basin.||||||
79350|Riverina Gneiss|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|3010-2600 Ma (inferred)||||Granitic gneiss; foliated and lineated|
79350|Riverina Gneiss|73596|6|Mentioned|p1155, 1164, 1170|Neoarchean|Mesoarchean|Ballard area, Kalgoorlie Terrane.|2812 +/- 8 Ma (Lu et al., 2018).|||||
25446|Robert Formation|41751|6|Mentioned|p8|||||||||
25446|Robert Formation|62453|6|Mentioned|p15|||Previously Robert Beds. Equivalent to Hussar Formation.||||||
25446|Robert Formation|65102|4|Described|p 364, 365,366,367,372 Figs. 4-41,4-43|Neoproterozoic|Neoproterozoic|Officer Basin. Few tens of metres; quartz arenite & feldspathic sandstone with minor chert; shallow marine, unconformably overlying granitic basement; type section at Breaden Bluff; unfossiliferous; correlated with Townsend Quartzite and Pindyin beds (S.A.).||||||
25446|Robert Formation|65416|6|Mentioned|p140.|||||||||
25449|Roebourne Group|22449|6|Mentioned|P25, Fig27 P26||Archean|Age of unit is 3270-3050 Ma||||||07-NOV-08
25449|Roebourne Group|23046|5|Briefly described|174|||Age ca 3270-3240 Ma. Overlying unit Cleaverville Formation||||||
25449|Roebourne Group|23244|6|Mentioned|Fig.1||Archean|of Hickman 1997. Oldest greenstones of west Pilbara Craton, deposited between ca.3270 and 3250 Ma. of of Pilbara Craton.||||||07-NOV-08
25449|Roebourne Group|23348|6|Mentioned|217|||||||||
25449|Roebourne Group|23484|5|Briefly described|p7|Archean|Archean|Of Pilbara Supergroup.  Age: 3270 -3250Ma.  See also page 10 table 2.||||||07-NOV-08
25449|Roebourne Group|23598|6|Mentioned|p5 Fig. 3|Paleoarchean|Paleoarchean|Geological Province: Pilbara Craton.||||||12-MAY-20
25449|Roebourne Group|23743|4|Described|p7|||Geological Province: Pilbara Craton.||||||
25449|Roebourne Group|23784|4|Described|p10|Archean|Archean|Intruded by Karratha Granodiorite.||||||07-NOV-08
25449|Roebourne Group|23789|5|Briefly described|p3|Archean|Archean|Age: 3270-3250Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
25449|Roebourne Group|23793|4|Described|p10|Archean|Archean|Age: 3270 - 3250 Ma||||||07-NOV-08
25449|Roebourne Group|23794|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
25449|Roebourne Group|23807|6|Mentioned|p109 Fig. 1|||Geological Province: Pilbara Craton.||||||
25449|Roebourne Group|23813|5|Briefly described|p89|Archean|Archean|Basalt, peridotite, chert, felsic volcanogenic metasediment.  Age: 3270-3260Ma. Geological Province: Pilbara Craton.  See also p91 Tb. 1||||||07-NOV-08
25449|Roebourne Group|23936|5|Briefly described|p2, Tb.1|Archean|Archean|Age: ca. 3250-3270 Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
25449|Roebourne Group|24023|5|Briefly described|p5|Archean|Archean|||||||07-NOV-08
25449|Roebourne Group|24024|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
25449|Roebourne Group|24160|6|Mentioned|p167 Fig.85.|Archean|Archean|Whim Creek area.|||||Metamorphosed sedimentary rock.|
25449|Roebourne Group|24166|5|Briefly described|p3|Archean|Archean|||||||07-NOV-08
25449|Roebourne Group|24184|4|Described|p710, p711 Tb.1|Neoarchean|Neoarchean|Geological Province: Pilbara Craton. Age: ca.3270-3250Ma||||||07-NOV-08
25449|Roebourne Group|24185|5|Briefly described|p735 Fig.2, p737 Tb.2|Archean|Archean|Age: 3.27-3.24 Ga. Geological Province: Pilbara Craton.||||||07-NOV-08
25449|Roebourne Group|24353|4|Described|p5|Archean|Archean|Age: c.3270-3250Ma. Geological Province: Pilbara Craton||||||07-NOV-08
25449|Roebourne Group|24541|1|Redefined|p1, p11 Tb.2, p15|Archean|Archean|Of the Pilbara Supergroup. Geological Province: West Pilbara Granite-Greenstone Terrane. Age: c. 3270-3250 Ma. Redefined to exclude the Regal Formation (Hickman, in prep.a).||||||23-DEC-09
25449|Roebourne Group|24543|5|Briefly described|Map legend|Archean|Archean|Of the Pilbara Supergroup.  Age: c.3270-3250Ma.||||||07-NOV-08
25449|Roebourne Group|24550|5|Briefly described|p36 Tb. 3.2|Archean|Archean|Basalt, chert, volcanic sediments and granodiorite. Age: 3270-3260Ma. Geological Province: Pilbara Craton. See p74 Tb. 5.1.||||||07-FEB-11
25449|Roebourne Group|24590|6|Mentioned|p28 Fig. 1.2|||Geological Province: Pilbara Craton.||||||07-FEB-11
25449|Roebourne Group|30766|6|Mentioned|p6|||||||||
25449|Roebourne Group|30882|4|Described|p50|||Stratigraphy||||||
25449|Roebourne Group|31393|6|Mentioned|Pl.25|||||||||
25449|Roebourne Group|31828|6|Mentioned|p33|||Metasediments, amphibole grade||||||
25449|Roebourne Group|31853|6|Mentioned|Table 9|||Refers Ryan (1964,1965)||||||
25449|Roebourne Group|36257|6|Mentioned|Fig.2.4|||||||||
25449|Roebourne Group|37373|4|Described|p75|||||||||
25449|Roebourne Group|44477|5|Briefly described|p.6|||SF/50-6.||||||
25449|Roebourne Group|44478|14|Not recorded|map legend||Archean|||||||07-NOV-08
25449|Roebourne Group|44501|14|Not recorded|p.7,10, Table 2, map||Archean|(ref to Ryan 1964). (F/50-7).||||||07-NOV-08
25449|Roebourne Group|44502|14|Not recorded|map legend||Archean|||||||07-NOV-08
25449|Roebourne Group|44536|14|Not recorded|map legend||Archean|||||||07-NOV-08
25449|Roebourne Group|45086|6|Mentioned|p14|||Precamb. Lithology.||||||
25449|Roebourne Group|50382|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
25449|Roebourne Group|50430|5|Briefly described|p153||Archean|3280-3250 Ma. In Karratha Domain.||||||07-NOV-08
25449|Roebourne Group|61253|5|Briefly described|p53, p52 Fig. 2, p58|Archean|Archean|Together with the Karratha Granodiorite in the West Pilbara Granite-Greenstone Terrane, interpreted to be a rifted segment of Sulphur Springs/Cleland Supersuite of the East Pilbara Granite-Greenstone Terrane.  Age: 3.28-3.25Ga. Geol.Prov: Pilbara Craton.||||||07-NOV-08
25449|Roebourne Group|61267|5|Briefly described|p71, p72 Fig.1|Archean|Archean|Intruded by the Karratha Granodiorite. Age: c. 3270-3050 Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
25449|Roebourne Group|63441|5|Briefly described|p5 Tb. 1, p24|Archean|Archean|Of Pilbara Supergroup. Comprises Ruth Well and Nickol River Formations. Age: 3.27Ga.  In the Karratha Terrane, West Pilbara Superterrane.||||||07-FEB-11
25449|Roebourne Group|63538|4|Described|p2 Fig. 1, p5, p22, p29, p9 Fig. 3|Archean|Archean|Includes Ruth Well and Nickol River Formations. ?Overlain by Regal Formation. Age: 3270-3275 Ma. Geological Province: Pilbara Craton. Ultramafic to felsic volcanic and sedimentary rocks.||||||19-APR-13
25449|Roebourne Group|63649|5|Briefly described|p200 Fig. 1|Archean|Archean|Geological Province: West Pilbara Terrane/ Karratha Terrane.||||||07-FEB-11
25449|Roebourne Group|64174|5|Briefly described|Map legend|Archean|Archean|Includes Ruth Well and Nickol River Formations. Age range: 3269-3251Ma.||||||07-NOV-08
25449|Roebourne Group|64580|6|Mentioned|map legend|||||||||
25449|Roebourne Group|64632|6|Mentioned|p201 Fig.1|Paleoarchean|Paleoarchean|Karratha Terrane (3.27-3.25 Ga), West Pilbara Superterrane||||||
25449|Roebourne Group|66118|5|Briefly described|p146 Fig.1|||Pilbara Craton. West Pilbara Superterrane. Karratha Terrane.|>= 3260 Ma|||||
25449|Roebourne Group|66217|5|Briefly described|p9.|Paleoarchean|Paleoarchean|Karratha Terrane.|3.27-3.25 Ga.|||||
25449|Roebourne Group|67201|4|Described|p3, p7, p10, p12-14, see comments|Archean|Archean|In northwestern Pilbara Craton, West Pilbara Superterrane, Karratha Terrane. Previously Nickol River Formation (along with Ruth Well Formation). Tectonic contacts above and below. Page location continued: p16-17, p26, p37, p67.|3300-3220 Ma||Nickol River Formation, Ruth Well Formation|Regal Thrust Zone lies between overlying Regal Formation and underlying Nickol River Formation. Correlated with Sulphur Springs Group and Cleland Supersuite.||25-NOV-16
25449|Roebourne Group|67269|6|Mentioned|p2 Fig.1|Paleoarchean|Paleoarchean|Karratha Terrane, W. Pilbara Superterrane.||||||
25449|Roebourne Group|67888|6|Mentioned|p50|||||||||
25449|Roebourne Group|68035|6|Mentioned|p285 Fig 2|||Karratha Terrane, West Pilbara Superterrane.||||||
25449|Roebourne Group|68284|6|Mentioned|p2|||West Pilbara Superterrane.|||||Granitic rocks.|
25449|Roebourne Group|69185|5|Briefly described|500k_geologyp08_lut.csv|||Geological Province: Pilbara Craton.|||Includes Nickol River Formation, Regal Formation, Ruth Well Formation.|||
25449|Roebourne Group|69301|4|Described|p3 Fig.1, p5 Fig.3, p9 Tb.1, p20 Tb.2|||Pilbara Craton. West Pilbara Superterrane. Karratha Terrane.|3270-3250 Ma from unit ages||Nickol River Formation, Ruth Well Formation||Granitic rocks.|
25449|Roebourne Group|70022|6|Mentioned|p114-115|||Karratha Terrane, West Pilbara Superterrane.|3280 Ma.|De Grey Supergroup.|Ruth Well Formation.|||
25449|Roebourne Group|70775|5|Briefly described|p6, p10, p12-p13, p15|Paleoarchean|Paleoarchean|Karratha Terrane. Originally defined to comprise the Ruth Well Formation and the Nickol River Formation (Hickman., 1997a) it has since been redefined to comprise only the Ruth Well Formation and the Weerianna Basalt. Interpreted to have been the product of a mantle plume and hosts archean Ni-Cu minerlization. See also p19-p20, p22-p26, p32, p39, p44 fig 27, p52, p69, p72-p73, p99.|c. 3280 Ma||Includes the Weerianna Basalt and the Ruth Well Formation.|Unconformably overlain by the Nickol River Formation. Intruded by the Karratha Granodiorite.||
25449|Roebourne Group|70826|6|Mentioned|p6 tbl 2, p8|Paleoarchean|Paleoarchean|Karratha Terrane. Temporally equivalent to the Sulphur Springs Group.||||Intruded by Cleland Supersuite. Unconformably overlain by Nickol River Formation.||12-MAY-20
25449|Roebourne Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||komatiite, peridotite, chert, basalt|
25449|Roebourne Group|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||||||Basalt and komatiite; minor chert; metamorphosed.|
25449|Roebourne Group|72251|5|Briefly described|p52,54|Paleoarchean|Paleoarchean|Geological province: Karratha Terrane, West Pilbara Superterrane, Pilbara Craton.|3280 Ma||Includes Ruth Well Formation.|Overlain unconformably by Nicol River Formation.||
25449|Roebourne Group|72668|5|Briefly described|p2, p3-4, p11-13, p28|||Karratha Terrane of the West Pilbara Superterrane. Contemporaneous with the intrusion of the Karratha Granodiorite. Continental setting.|3270-3250 Ma||Includes the Nickol River Formation and the Ruth Well Formation.|Coeval with the Cleland Supersuite.|Ultramafic to felsic volcanic and sedimentary rocks.|13-JAN-22
36126|Roebourne Lithotectonic Complex|23455|5|Briefly described|p43|Archean|Archean|||||||07-NOV-08
34565|Rosabrook Coal Measures|12758|4|Described|p13, p3 Fig.3, p8 Fig.9. p57|Early Permian|Early Permian|Of the Sue Group. Characterised by poorly sorted feldspathic sandstone intercalated with siltstone and carbonaceous shale grading up into coal.  Conformably overlain by Ashbrook Fm; conformably underlain by Woodynook Sst.  Thickness in type section: 241m.||||||29-APR-09
34565|Rosabrook Coal Measures|14227|5|Briefly described|Enclos. 2|Artinskian|Sakmarian|Of the Sue Group. Overlies Woodynook Sandstone; underlies Ashbrook Formation. Geol. Prov: Bunbury Trough, southern Perth Basin.||||||07-FEB-11
34565|Rosabrook Coal Measures|22818|5|Briefly described|map|Early Permian|Early Permian|Sue Group||||||
34565|Rosabrook Coal Measures|22819|5|Briefly described|map|Early Permian|Early Permian|Sue Group||||||
34565|Rosabrook Coal Measures|22820|2|Defined|p9, Tb. 2, p17, p25, p30|Early Permian|Early Permian|Of Sue Group. Contains 9 named. Thickness:130-240m. Conformable below Ashbrook Sandstone. Geol.prov: S. Perth Basin. Cluster of moderately thick coal seams intercalated with poorly sorted feldspathic sst, siltst.+ carbonaceous shale. Detailed lith.||||||12-AUG-08
34565|Rosabrook Coal Measures|24443|5|Briefly described|Fig.31|Early Permian|Early Permian|Of Sue Group. Conformably overlies Woodynook Sandstone. Conformably overlain by Ashbrook Sandstone. Geological Province: Perth Basin.||||||
34565|Rosabrook Coal Measures|50107|5|Briefly described|Map legend|Permian|Permian|Of the Sue Group. Geological Province: Southern Perth Basin.||||||28-JUL-09
34565|Rosabrook Coal Measures|60386|6|Mentioned|p296|||Perth Basin. Shown as Early Permian. Non-marine, coal.||||||
34565|Rosabrook Coal Measures|64630|5|Briefly described|p31 Fig.2|Artinskian|Sakmarian|Province: Southern Perth Basin. Overlies the Woodynook Sandstone, underlies the Ashbrook Sandstone. Palynology age: P. pseudoreticulata to M. trisina.||||||23-JUL-15
34565|Rosabrook Coal Measures|67925|4|Described|Ch2 p10 fig 4, Ch2 p11-p12|Artinskian|Sakmarian|A type section in the Sue 1 drillhole is 198m thick. Interpreted to have been deposited in a fluvial-plain setting in which deltas prograded into a lacustrine environment. Palynology discussed. See also Ch2 p15, Ch2 p20, Ch2 p26-p27, Ch2 p30, Ch3 p8, Ch4 p8 fig 2.||Sue Group||Conformably overlies the Woodynook Sandstone. Overlain by the Ashbrook Sandstone.|Poorly sorted feldspathic sandstone that is intercalated with siltstone and carbonaceous shale grading into coal.|
34565|Rosabrook Coal Measures|69029|6|Mentioned|p332|Artinskian|Artinskian|Of Perth Basin.||||Overlain by Irwin River Coal Measures. Underlain by High Cliff Sandstone.||
34565|Rosabrook Coal Measures|69081|5|Briefly described|p737 Fig.1|Cisuralian|(IV) D a|Presented as Rosabrook Coal Ms in figure. Geol. Prov: Perth Basin.||Sue Group||Is overlain by Ashbrook Sandstone; overlies Woodynook Sandstone.||23-JUL-15
34565|Rosabrook Coal Measures|69182|6|Mentioned|Ch2 p9, Ch2 p11, Ch2 p45, Ch2 p47-p49|Early Permian|Early Permian|Perth Basin. Age equivalent of the Irwin River Coal Measures. See also  Ch2 p55, Ch2 p57, Ch2 p60-p66, Ch2 p80, Ch2 p84, Ch2 p91, Ch2 p92, Ch2 p94-p96, Ch2 p98, Ch2 p100, Ch2 p102, Ch2 p104, Ch2 p106, Ch2 p108, Ch2 p110.||Sue Group||Overlies the Woodynook Sandstone. Overlain by the Ashbrook Sandstone.||
34565|Rosabrook Coal Measures|69297|6|Mentioned|p175, p187, p189|Kungurian|Artinskian|Vlaming Sub-basin, South Perth Basin. ||Sue Group||Overlies the Woodynook Sandstone. Overlain by the Ashbrook Sandstone.||
34565|Rosabrook Coal Measures|70097|5|Briefly described|p2, p19 Fig.3|Artinskian|Sakmarian|Southern Perth Basin. Bunbury Trough.||Sue Group||Overlies Woodynook Sandstone. Is overlain by Ashbrook Sandstone.|Deltaic sediments basin fill. Includes coal.|12-SEP-17
34565|Rosabrook Coal Measures|70099|5|Briefly described|Fig.4|Kungurian|Sakmarian|||Sue Group.||Overlies Woodynook Sandstone. Is overlain by Ashbrook Sandstone.||
34565|Rosabrook Coal Measures|70128|5|Briefly described|p449|Permian|Permian|Southern Perth Basin.||Sue Group.||Conformably overlies Woodynook Sandstone. Is overlain conformably by Ashbrook Sandstone.||
34565|Rosabrook Coal Measures|70774|5|Briefly described|p5 fig 3|Artinskian|Sakmarian|Southern Perth Basin.||||Overlies the Woodynook Sandstone. Overlain by the Ashbrook Sandstone.||
34565|Rosabrook Coal Measures|71146|5|Briefly described|p6, p39,  p43 fig 33|Kungurian|Artinskian|Perth Basin.||||Overlies the Woodynook Sandstone. Overlain by the Ashbrook Sandstone.|Mixed sandstone, mudstone and coal.|
34565|Rosabrook Coal Measures|71377|5|Briefly described|p7|Permian|Permian|Perth Basin.||Stockton Group||||
34565|Rosabrook Coal Measures|71958|5|Briefly described|p34|Artinskian|Sakmarian|Vlaming Sub-basin.||Sue Group||Overlies the Woodynook Sandstone. Overlain by the Ashbrook Coal Measures.||
34565|Rosabrook Coal Measures|72258|5|Briefly described|p129|Cisuralian|Cisuralian|Of Perth Basin.||||Overlain by Ashbrook Sandstone. Underlain by Woodynook Sandstone. Laterally grades into Holmwood Shale.||
22781|Rose Bore Granite|22547|5|Briefly described|p13|Orosirian|Orosirian|Age: 1863 +/- 3 Ma.||||||14-NOV-06
22781|Rose Bore Granite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Age: c.1865Ma.||||||07-NOV-08
22781|Rose Bore Granite|23751|5|Briefly described|p12|Paleoproterozoic|Paleoproterozoic|Age: c.1863 Ma.||||||07-NOV-08
22781|Rose Bore Granite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tickalara Metamorphics (Lamboo Complex).  Age: 1865-1850Ma.||||||07-NOV-08
22781|Rose Bore Granite|43854|5|Briefly described|Map Legend||Proterozoic|of Tickalara Metamorphics.||||||28-NOV-07
22781|Rose Bore Granite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
22781|Rose Bore Granite|50437|5|Briefly described|p3.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Age: 1863 +/- 3Ma (SHRIMP).||||||22-SEP-14
22781|Rose Bore Granite|63866|5|Briefly described|p131, p138|Orosirian|Orosirian||ca 1863 Ma (Page and Hoatson, 2000)|||Intrudes the Tickalara Metamorphics.||
22781|Rose Bore Granite|64730|6|Mentioned|p141|Orosirian|Orosirian|Of Central Zone of the Halls Creek Orogen (Tyler and Page 1996).|1863 Ma.|||||03-MAY-12
22781|Rose Bore Granite|66845|4|Described|p538, p539 Tb.1|||Protoliths of Tickalara Metamorphics were intruded by leucogranite sheets, named Rose Bore Granite and Fletcher Creek Monzogranite ("Eastern Leucocratic Granitoid" of Ogasawara, 1988). This unit predates earliest deformation in Central zone (D1) of Lamboo Complex.|1863+/-3 Ma U-Pb SHRIMP zircon Page & Hoatson 2000||||Migmatitic granite.|04-AUG-15
22781|Rose Bore Granite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Data from OZCHRON1. Comment: 'This is the igneous crystallisation age based on 18 of the 21 analyses. The data are concordant.'|1863+/-3 Ma U/Pb SHRIMP|Tickalara Metamorphics|||Foliated biotite-muscovite metasyenogranite and felsic gneiss; locally migmatitic and sillimanite bearing.|04-AUG-15
22781|Rose Bore Granite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv. |1863 Ma||||Foliated biotite--muscovite metasyenogranite and felsic gneiss; locally migmatitic and sillimanite bearing.|
22781|Rose Bore Granite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Central Zone.|1863-1863 Ma (Isotopic)|Unit of Tickalara Metamorphics.|||Foliated biotite-muscovite metasyenogranite and felsic gneiss; locally migmatitic and sillimanite bearing|
22781|Rose Bore Granite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1856 Ma||||Foliated biotite-muscovite metasyenogranite and felsic gneiss; locally migmatitic and sillimanite bearing.|
22781|Rose Bore Granite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1863+\-3 Ma (isotopic)|Unit of Tickalara Metamorphics.|||Foliated biotite-muscovite metasyenogranite and felsic gneiss; locally migmatitic and sillimanite bearing|
22781|Rose Bore Granite|71873|5|Briefly described|p441-443|Orosirian|Orosirian|Geological province: Lamboo Province.  Deformed by Hooper Orogeny c. 1860 Ma. TTG-granitic suite coeval with the Panton intrusion, coinciding with Paperbark Supersuite, Ruins Dolerite and Whitewater Volcanics, which reflects the suturing of the Western and Central zones during the amphibolite-granulite facies Hooper Orogeny.|1863 Ma|Unit of Tickalara Metamorphics.||||
22781|Rose Bore Granite|72437|6|Mentioned|p6|Palaeoproterozoic|Palaeoproterozoic|Said to be the Blue Rock Granite of Sheppard et al 1995 who included it within the Dougalls suite; however the present authors have excluded it due to differing chemistry.|c. 1863 Ma|||||
79002|Rothsay Suite|70226|5|Briefly described|map legends|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Carton.|c.2749-c.2742 Ma (Fletcher and McNaughton, 2002).|Annean Supersuite|Goonetarra Granodiorite, Warbadoo Tonalite, Courin Granodiorite.||Metamorphosed granites, granodiorites, tonalites, monzogranites.|16-DEC-15
79002|Rothsay Suite|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton.|c.2749 Ma.|Annean Supersuite.|Goonetarra Granodiorite.|||
79002|Rothsay Suite|70770|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Three facies are mapped separately.|2756-2742 Ma.|Annean Supersuite.|||Granitic schist with abundant amphibolite rafts up to 50m long, locally strongly deformed; foliated biotite metamonzogranite, local K-feldspar phenocrysts; muscovite-rich granitic schist, biotite locally dominant, moderate cleavage.|07-MAR-17
79002|Rothsay Suite|70796|6|Mentioned|100k_geologyl_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100l_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 155822.1.pdf, 203702.1.pdf, 203703.1.pdf, 203704.1.pdf, 211102.1.pdf, Badja100_2240_stratig.pdf, Bungar100_2539_stratig.pdf, Yalgoo100_2241_stratig.pdf.|ca 2743 Ma (inferred)|Annean Supersuite|Includes the Warbadoo Tonalite and the Goonetarra Granodiorite.||Granitic schist with typically with a moderately developed cleavage. Foliated metamonzogranite; common pegmatite veins. Porphyritic to equigranular, medium to coarsegrained metagranodiorite. Granitic schist and metagranite.|
79002|Rothsay Suite|70826|6|Mentioned|p9|Neoarchean|Neoarchean|Youanmi Terrane.|||||Granites.|
79002|Rothsay Suite|70830|5|Briefly described|p9, p51|||Murchison Domain.||Annean Supersuite||||
79002|Rothsay Suite|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). Commonly exhibits a moderate to well-developed magmatic foliation, except near  greenstone contacts, where the primary fabric is overprinted by pervasive mylonitic deformation. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeol_lut.csv.|2756-2742 Ma|Unit of Annean Supersuite.|Includes Courin Granodiorite, Goonetarra Granodiorite, Warbadoo Tonalite.|Contains rafts of Bunnawarra Suite within plutons.|Granitic schist: muscovite rich, local biotite, amphibolite rafts; metamonzogranite: foliated biotite, porphyritic to equigranular, medium- to coarse-grained, magmatic foliation; foliated metagranite with dismemebered trains of amphibolite xenoliths|
79002|Rothsay Suite|71809|5|Briefly described|map legend|Archean|Archean|Yilgarn Craton, Youanmi Terrane||Of Annean Supersuite.|Includes Mulgine Granite.|||
79002|Rothsay Suite|73410|6|Mentioned|p2|||Youanmi Terrane.|2760-2740 Ma.||Goonetarra Granodiorite.|||
26877|Rottnest Limestone|23816|5|Briefly described|p256|Quaternary|Quaternary|Geological Province: Perth Basin. Age: 100 000 +/- 20 000 yrs B.P.||||||
26877|Rottnest Limestone|24160|6|Mentioned|p94|Quaternary|Quaternary|Perth Basin.||||||
26877|Rottnest Limestone|24410|5|Briefly described|p39|Quaternary|Quaternary|Of the Kwinana Group. Geological Province: Perth Basin.||||||
26877|Rottnest Limestone|32645|6|Mentioned|Map legend|late Pleistocene|late Pleistocene|||||||
26877|Rottnest Limestone|33044|6|Mentioned|p59|||||||||
26877|Rottnest Limestone|35093|3|Fully described|p15|||||||||
26877|Rottnest Limestone|36257|6|Mentioned|Table 2.1|||||||||
26877|Rottnest Limestone|36293|3|Fully described|p214|||||||||
26877|Rottnest Limestone|36890|5|Briefly described|p256|||||||||
26877|Rottnest Limestone|40400|6|Mentioned|p109|||Of Passmore (1970). Geological Province: Perth Basin.||||||06-AUG-07
26877|Rottnest Limestone|41751|6|Mentioned|p8|||||||||
26877|Rottnest Limestone|42569|6|Mentioned|p81|||||||||
26877|Rottnest Limestone|43310|5|Briefly described|Map Legend||Quaternary|||||||
26877|Rottnest Limestone|44144|4|Described|p501 Tb.4-21|Late Pleistocene|Late Pleistocene|Type Section: Fairbridge Bluff 32o00'58''S 115o30'48''E.  Over 3m thick coral reef sediments.|100 +/- 20 ka.|Kwinana Group||Interfingers with Tamala Limestone.|Coral reef and shell limestone.|
26877|Rottnest Limestone|63807|4|Described|p10-11|Late Pleistocene|Late Pleistocene|Coral reef limestone - as a thin intercalation overlain and underlain by Tamala Limestone. Thickness is 3m where exposed. Overlies herschell Limestone.||||||
26877|Rottnest Limestone|69558|6|Mentioned|p102|||Coral reef from last interglacial on Fairbridge Bluff, Rottnest Island.||||||25-MAY-21
26877|Rottnest Limestone|71958|5|Briefly described|p35|Late Pleistocene|Middle Pleistocene|Vlaming Sub-basin. Exposed in outcrops on the Rottnest islands. Forms a coral reef.||||Intercalated with the Tamala Limestone.||
80589|Round Hummock Dolerite|72712|5|Briefly described|p36, p38-40, p41.|Stenian|Stenian|A suite of W-NW dykes that are generally well exposed on the northern Pilbara Craton, where they have been dated at c. 1075 Ma (DAD Evans et al., written comm., 2016; Wingate, 2017). Difficult to distinguish from Moodagarra Dolerite on trend alone.|c. 1075 Ma.|||Cross cuts both Moodagarra and Panhandle Dolerites, hence younger.|Dolerite dykes.|
75984|Roundtop Komatiite|68520|5|Briefly described|Map legend|Archean|Archean|Southern Cross Domain, Youanmi Terrane, Yilgarn Craton. The 2 facies variants are mapped separately.|||||Komatiitic basalt with local pyroxene spinifex texture; komatiite with local olivine spinifex texture, minor cumulate and talc-tremolite schist: both metamorphosed.|
75984|Roundtop Komatiite|69559|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean|Southern Cross Domain, Youanmi Terrane, Yilgarn Craton. See also 100k_interpgeol_lut.csv, geologyp_lut.csv,  500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv,  geologyl_lut.csv.|2873-2720 Ma||||Komatiitic basalt; local pyroxene spinifex texture; minor cumulate and talc tremolite schist. Ultramafic schist also present.|
75984|Roundtop Komatiite|69617|5|Briefly described|p143, p145-149, p153-155|||Lake Johnston greenstone belt, Youanmi Terrane, Yilgarn Craton. Comprises three komatiitic units, described. The central such unit hosts the Maggie Hays nickel deposit, below the meta-BIF unit of the Honman Formation. Deposited betweeen 2879 Ma and 2765 or 2720 Ma; possible age discussed.||||Conformably overlies Honman Formation. Intrudes Maggie Hays and Honman Formations.||
75984|Roundtop Komatiite|70144|5|Briefly described|Map legend|Archean|Archean|Southern Cross Domain, Youanmi Terrane, Yilgarn Craton. The four facies are mapped separately.|||||Komatiitic basalt, local pyroxene spinifex texture; ultramafic schist, minor serpentinite and mafic schist; komatiite with local olivine spinifex texture, minor cumulate and schist; komatiite interleaved with ultramafic schist; all metamorphosed.|
75984|Roundtop Komatiite|70156|4|Described|GEOL_LUT_CSV files|Neoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3200-2600 Ma). See 500k_interpgeop14_lut.csv, 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeol_lut.csv.|2876-2720 Ma (inferred)||||Komatiite with local olivine spinifex texture; minor cumulate and talc--tremolite schist; metamorphosed|
75984|Roundtop Komatiite|70205|5|Briefly described|Map legend.|Archean|Archean|Southern Cross Domain, Youanmi Terrane, Yilgarn Craton. The two facies are mapped separately.|||||Metamorphosed komatiitic basalt with local pyroxene spinifex texture. Metamorphosed komatiite with local olivine spinifex texture, minor cumulate and talc-tremolite schist.|
75984|Roundtop Komatiite|70794|4|Described|100k_geologyp_lut.csv|Neoarchean|Mesoarchean|Youanmi Terrane, Yilgarn Craton.Age range 2876-2720 Ma shown in 500k_interpgeop14_lut.csv. See also 500k_interpgeop_lut.csv.|2920-2718 Ma inferred||||Komatiite with local olivine spinifex texture or local pyroxene spinifex texture; minor cumulate and talc-tremolite schists; metamorphosed. Komatiite, metamorphosed, interleaved with ultramafic schist; includes talc--tremolite--chlorite schist|
75984|Roundtop Komatiite|70802|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Youanmi Terrane events.|2876-2720 Ma (inferred)||||Komatiite with local olivine spinifex texture; minor cumulate and talc--tremolite schist; metamorphosed|
75984|Roundtop Komatiite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Mesoarchean|Youanmi Terrane.|||||Komatiite with local olivine spinifex texture; minor cumulate and talc--tremolite schist; metamorphosed.|
28275|Rouse Creek Arenite|23311|5|Briefly described|map legend|Proterozoic|Proterozoic|Of Uaroo Group.||||||
28275|Rouse Creek Arenite|37016|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
28275|Rouse Creek Arenite|39427|2|Defined|p4|Precambrian|Precambrian|||||||
28275|Rouse Creek Arenite|40900|6|Mentioned|p32|||||||||
28275|Rouse Creek Arenite|41360|6|Mentioned|p192|||||||||
28275|Rouse Creek Arenite|44142|5|Briefly described|p326 Tb.4-5|||1000m thick.||Uaroo Group.||Correlates with Gooragoora Sandstone.|Quartz arenite.|
28275|Rouse Creek Arenite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, crystalline dolostone/dolomite|
80170|Rowland Suite|71211|4|Described|p26, p27 fig 2.3,|Stenian|Stenian|Consists of a number of mineralogically and geochemically related intrusive pophyritic rhyolites. Generally <250m thick. On the basis of geochemistry is interpreted to be genetically related to the Alcurra Dolerite Suite, Hogarth Formation and the Kathleen Ignimbrite. I.e. it is believed to be a primitive crystal rich cumulate end-member related to the more evolved Kathleen Ignimbrite and the more primitive Alcurra Dolerite Suite. Referred to as the RS periodically throughout the text. See also p28, p64 fig 2.16, p67, p68, p81, p82, p86-p88, p88 fig 3.3, p90, p94, p96, p98-p101, p103, p104, p106, p108, p108 fig 3.11, p110-p113, p116-p117, p120, p135, p137 fig 4.2, p138, p144, p147, p150, p182-p183, p208-p210, p213, p216, p218, p243, p249, p253, p270.|1062 +/- 8 Ma to 1078 +/- 5 Ma|Pussy Cat Group [??]||Intrudes the Pussy Cat Group, Cleghorne Formation, Kathleen Ignimbrite and the Glyde Formation.|Crystal-rich, porphyritic or phaneritic, quartz-feldspar rhyolitic intrusions.|05-JUL-22
38090|Roy Hill Member|23570|4|Described|p129, p239 Appendix 1|||Abbreviation of Roy Hill Shale Member.||||||12-DEC-12
38090|Roy Hill Member|66685|6|Mentioned|p217 Fig.2|Archean|Archean|||Jeerinah Formation||Overlies the Warrie Member.||
38090|Roy Hill Member|67201|5|Briefly described|p29 Fig.15, p34 Fig.18|||Northern Fortescue Basin, Northeast and Northwest Pilbara Sub-basins.||Jeerinah Formation||||
38090|Roy Hill Member|69301|5|Briefly described|p18 Fig.7|||Pilbara Craton. Fortescue Basin. Northeast Pilbara Sub-basin, Northwest Pilbara Sub-basin, Sequence 4. ||Jeerinah Formation||||
38090|Roy Hill Member|69563|5|Briefly described|p690, p692-693|||Contains what the authors call the Jeerinah Impact Layer, a 1-6mm thick microkrystite spherule unit, overlain by the Marra Mamba Iron Formation. Appears as Roy Hill Shale on p692.||Unit in Jeerinah Formation.||||
38090|Roy Hill Member|70733|6|Mentioned|p120|||||Fortescue Group.||||
25454|Royal Amphibolite Member|30562|4|Described|p39|||Refers Hall & Bekker (1965). See also P37||||||
25454|Royal Amphibolite Member|43162|6|Mentioned|6|||||||||
35660|Royal Hill Member|23126|5|Briefly described|p383 Fig.3|||||||||
72594|Royal Sandstone|66880|6|Mentioned|p14 Table 3, p12 Table 2|Archean|Archean||2658 +/- 15 Ma.|||||01-NOV-12
29420|Roysalt Formation|14227|5|Briefly described|Enclos. 2|Pliocene|Late Miocene|Presented as Polar Bear, Roysalt FMS.||||||07-FEB-11
29420|Roysalt Formation|22769|5|Briefly described|Table1p759||Holocene|||||||
29420|Roysalt Formation|42959|4|Described|p63|||See also Fig.3 p58||||||
29420|Roysalt Formation|43761|4|Described|p420-421|Early Pliocene|Late Miocene|||||||
29420|Roysalt Formation|43838|6|Mentioned|p4||Tertiary|Within Redmine Group||||||12-JUL-16
29420|Roysalt Formation|61155|5|Briefly described|p17|Holocene|Early Pliocene|Age: <5Ma. Thickness: 9m. Geological region: Norseman region. ||||||
29420|Roysalt Formation|64646|6|Mentioned|p23 Fig. 3, p24 Fig. 4|Pliocene|Pliocene|Geological Province: Yilgarn Craton.||||||08-FEB-10
29420|Roysalt Formation|65194|5|Briefly described|p136 Fig.4.37, p137|||Caps the sediments in the Lefroy Palaeovalley. Gypsum-bearing evaporites. Includes Beta Island Member. Likely formed in the Quaternary.||||||
29420|Roysalt Formation|69598|6|Mentioned|p2, p9, p10, p11 Tb.1, p29 Tb.4|Pleistocene|Pliocene|Eucla Basin. Typically no more than 10m thick. ||Redmine Group||||
74910|Rubberoid Granite|66105|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Moorarie Supersuite. Pale grey, medium- to coarse-grained, seriate to porphyritic metamonzogranite; typically with well-developed igneous layering; commonly with mingled pegmatite veins; minor mesocratic metagranodiorite; locally schistose.||||||
74910|Rubberoid Granite|66110|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Moorarie Supersuite. Pale grey, medium- to coarse-grained, seriate to porphyritic metamonzogranite; typically with well-developed igneous layering; commonly with mingled pegmatite veins; minor mesocratic metagranodiorite; locally schistose.||||||
74910|Rubberoid Granite|66299|4|Described|p13, p173, pp177-178.|Paleoproterozoic|Paleoproterozoic|Undeformed, but magmatically layered granites composed of hundreds or thousands of individual magma batches.|1791 +/- 4 Ma to 1786 +/- 6 Ma.|Unit in Moorarie Supersuite.||Intrudes Middle Spring Granite and Leake Spring Metamorphics.|Pale grey, medium- to coarse-grained, seriate to porphyritic metamonzogranite, typically with well-developed igneous layering; commonly with mingled pegmatite veins; minor mesocratic metagranodiorite; locally schistose.|
74910|Rubberoid Granite|68521|5|Briefly described|Map Legend|Statherian|Orosirian|Geochronology from Evans et al. (2003).|c.1830-1780 Ma|Of the Moorarie Supersuite.|||Pale-grey, medium-grained, seriate to porphyritic metamonzogranite; typically with well-developed igneous layering; commonly with mingled pegmatite veins; minor mesocratic metagranodiorite; locally schistose.|
74910|Rubberoid Granite|68522|5|Briefly described|Map Legend|Statherian|Orosirian|Gascoyne Province. |1820-1775 Ma|Of the Moorarie Supersuite.|||Pale-grey, medium- to coarse-grained, seriate to porphyritic metamonzogranite; typically with well-developed igneous layering; commonly with mingled pegmatite veins; minor mesocratic metagranodiorite; locally schistose.|
74910|Rubberoid Granite|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|||Moorarie Supersuite|||Pale-grey, medium- to coarse-grained, seriate to porphyritic metamonzogranite; typically with well-developed igneous layering; commonly with mingled pegmatite veins; minor mesocratic metagranodiorite; locally schistose|
74910|Rubberoid Granite|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|100k_interpgeop_lut.csv|1791-1786 Ma||||Medium to coarse grained, seriate to porphyritic metamonzogranite; typically with well developed igneous layering; commonly with mingled pegmatite veins; minor mesocratic metagranodiorite; locally schistose.|
74910|Rubberoid Granite|71869|5|Briefly described|p6|||Capricorn Orogen.|1791 +/- 4 Ma (igneous cryst. Age)|Moorarie Supersuite|||Metamonzogranite.|
30278|Ruby Plains Group|22496|4|Described|p10|Neoproterozoic|Neoproterozoic|Comprises Mount Kinahan Sandstone, Eliot Range Dolomite and Illjarra Sandstone.  Geological Province:  Wolfe Basin.||||||
30278|Ruby Plains Group|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
30278|Ruby Plains Group|22754|5|Briefly described|p5 Tb. 1|Neoproterozoic|Neoproterozoic|Geological Province: Wolfe Creek Basin.||||||
30278|Ruby Plains Group|22777|5|Briefly described|Map|||||||||
30278|Ruby Plains Group|22899|6|Mentioned|86|||||||||
30278|Ruby Plains Group|23314|4|Described|330||Neoproterozoic|Of Wolfe Basin.||||||
30278|Ruby Plains Group|23621|2|Defined|p55 Appendix|Cryogenian|Tonian|See also page 32, 9 Table 1. Type section included. Overlying unit Duerdin Group (disconformably). Underlying unit Olympio Formation. Geological Province: Wolfe Basin. Max. thickness: 1000 m.||||||18-MAY-15
30278|Ruby Plains Group|23622|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Age: c800 Ma. Geological Province: Wolfe Basin.||||||
30278|Ruby Plains Group|24173|3|Fully described|p24, p11 Tb.2|Tonian|Tonian|Comprises Mount Kinahan Sandstone, Eliot Range Dolomite and Illjara Sandstone. Unconformably overlain by Duerdin Group; unconformably overlies Halls Creek Group.  Age: 800-700Ma Geological Province: Wolfe Basin.||||||06-APR-05
30278|Ruby Plains Group|24503|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Sandstone, dolomite, stromatolitic dolomite, dolomitic mudstone, mudstone and siltstone.  Geological Province: Wolfe Creek Basin.||||||
30278|Ruby Plains Group|43303|5|Briefly described|Map Legend||Neoproterozoic|||||||
30278|Ruby Plains Group|44868|5|Briefly described|Map Legend||Phanerozoic|||||||
30278|Ruby Plains Group|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes: Illjarra Sandstone, Eliot Range Dolomite, Mount Kinahan Sandstone. Geological Province: Wolfe Creek Basin.||||||03-NOV-04
30278|Ruby Plains Group|60533|5|Briefly described|p605|Cryogenian|Tonian|Geological Province: Wolfe Basin.||||||
30278|Ruby Plains Group|64104|6|Mentioned|p76 fig 10, p77|Neoproterozoic|Neoproterozoic||||Includes Eliot Range Formation.|||
30278|Ruby Plains Group|64580|4|Described|map legend|Neoproterozoic|Neoproterozoic|Sandstone, dolomite, stromatolitic dolomite, dolomitic mudstone, mudstone, and siltstone.||||||15-DEC-08
30278|Ruby Plains Group|64724|5|Briefly described|p49 Fig. 7|Cryogenian|Cryogenian|Deposited in the Wolfe Basin during the Centralian 1 event (~840-824 Ma)||||||
30278|Ruby Plains Group|64793|6|Mentioned|p291|||From the Kimberley.||||||
30278|Ruby Plains Group|68244|6|Mentioned|p666|Neoproterozoic|Neoproterozoic|East Kimberly area, Kimberley region. Wolfe Creek Basin.|||Includes Eliot Range Dolomite.|Overlain unconformably by Duerdin Group.||21-JUN-19
30278|Ruby Plains Group|68656|5|Briefly described|GEOL_LUT_CSV/500k_geologyp08_lut|Neoproterozoic|Neoproterozoic|Wolfe Creek Basin, Halls Creek Orogen. See also 500k_intergeop_lut.csv|||||Undivided; sandstone, dolomite, stromatolitic dolomite, dolomitic mudstone, mudstone and siltstone.|
30278|Ruby Plains Group|68733|5|Briefly described|p189 Fig.8|Cryogenian|Cryogenian|Wolfe Basin.|||Includes Eliot Range Dolomite and Mount Kinahan Sandstone.|||
30278|Ruby Plains Group|69099|4|Described|GEOL_LUT_CSV files + geochron files|Cryogenian|Cryogenian|Wolfe Creek Basin|||Includes Illjarra Sandstone, Eliot Range Dolomite, Mount Kinahan Sandstone.||Sandstone, dolomite, stromatolitic dolomite, dolomitic mudstone, mudstone, and siltstone.|04-AUG-15
30278|Ruby Plains Group|69165|4|Described|100k_interpgeop_lut.csv|Neoproterozoic|Neoproterozoic|See also 500k_geologyp08_lut.csv. |||Includes Illjarra Sandstone, Eliot Range Dolomite, Mount Kinahan Sandstone||Undivided; sandstone, dolomite, stromatolitic dolomite, dolomitic mudstone, mudstone and siltstone.|
30278|Ruby Plains Group|69442|6|Mentioned|p27:1|||Wolfe Basin.||||||12-JUL-16
30278|Ruby Plains Group|69587|4|Described|GEOL_LUT_CSV files|Cryogenian|Cryogenian|Geological province: Halls Creek Orogen, North Australian Craton. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1. See 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|830-810 Ma (inferred)||||Sandstone, dolomite, stromatolitic dolomite, dolomitic mudstone, mudstone, and siltstone|
30278|Ruby Plains Group|69634|4|Described|GEOL_LUT_CSV files|Neoproterozoic|Neoproterozoic|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|830-810 (Inferred)||Includes Eliot Range Dolomite, Illjarra Sandstone, Mount Kinahan Sandstone.||Undivided; sandstone, dolomite, stromatolitic dolomite, dolomitic mudstone, mudstone, and siltstone|
30278|Ruby Plains Group|70154|6|Mentioned|100k_interpgeop_lut.csv|Cryogenian|Neoproterozoic||||Includes Illjarra Sandstone, Eliot Range Dolomite, Mount Kinahan Sandstone|||
30278|Ruby Plains Group|70851|6|Mentioned|p18-p19, p36|||||||||
30278|Ruby Plains Group|71267|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|1000-720 Ma (inferred)||Includes Eliot Range Dolomite, Illjarra Sandstone., Mount Kinahan Sandstone||Sandstone, dolomite, stromatolitic dolomite, dolomitic mudstone, mudstone, and siltstone|
30278|Ruby Plains Group|72034|5|Briefly described|500k_interpgeop16_lut|Tonian|Tonian|Wolfe Basin.|||||Sandstone, dolomite, stromatolitic dolomite, dolomitic mudstone, mudstone, and siltstone.|
26880|Rudall Complex|22716|6|Mentioned|table4, p229,237,238|Paleoproterozoic|Paleoproterozoic|Eastern third formed by the Tabletop Terrane.||||||09-JUL-13
26880|Rudall Complex|22816|5|Briefly described|p10 Fig. 4|Mesoproterozoic|Mesoproterozoic|Gibson Sub-Basin||||||
26880|Rudall Complex|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Stratigraphic succession incompletely determined. Paterson Orogen.||||||
26880|Rudall Complex|23571|6|Mentioned|p4 Fig. 2|||Geological Province: Officer Basin||||||
26880|Rudall Complex|23585|6|Mentioned|p22|||Overlying unit Throssell Group.||||||
26880|Rudall Complex|23590|4|Described|p7|Paleoproterozoic|Paleoproterozoic|>1760 Ma. Overlying unit Throssell Group. Geological Province: Paterson Orogen.||||||07-NOV-08
26880|Rudall Complex|23602|4|Described|p7|||||||||
26880|Rudall Complex|23722|6|Mentioned|p24|||||||||
26880|Rudall Complex|23723|6|Mentioned|p6 Fig 2|||||||||
26880|Rudall Complex|23729|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province:  Paterson Orogen.||||||
26880|Rudall Complex|23730|4|Described|p7|Paleoproterozoic|Paleoproterozoic|Age: >1760 Ma. Overlying unit Throssell Group. Geological Province: Paterson Orogen.||||||07-NOV-08
26880|Rudall Complex|23742|4|Described|p4|Paleoproterozoic|Paleoproterozoic|Geological Province: Paterson Orogen.||||||07-NOV-08
26880|Rudall Complex|23745|6|Mentioned|p5 Fig 3|||||||||
26880|Rudall Complex|23746|6|Mentioned|p27|||||||||
26880|Rudall Complex|23758|5|Briefly described|p2 Fig 1|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26880|Rudall Complex|23760|4|Described|p8|Paleoproterozoic|Paleoproterozoic|Geological Province: Paterson Orogen.||||||07-NOV-08
26880|Rudall Complex|23784|5|Briefly described|p4 Tb. 1|Archean|Archean|||||||07-NOV-08
26880|Rudall Complex|23900|4|Described|p1536|Paleoproterozoic|Paleoproterozoic|Unconformably overlain by the Yeneena Supergroup. Geological Province: Paterson orogen. See also Rudall Metamorphic Complex.||||||07-NOV-08
26880|Rudall Complex|24115|5|Briefly described|p28|Mesoproterozoic|Mesoproterozoic|Age: c. 1490 Ma.||||||
26880|Rudall Complex|24194|4|Described|p898, p899 Fig.2, p900, Fig.3|Paleoproterozoic|Paleoproterozoic|See also Rudall Metamorphic Complex. Overlying Unit: Yeneena Supergroup. Geological Province: Yeneena Basin.||||||07-NOV-08
26880|Rudall Complex|24197|5|Briefly described|p100|||Comprises older banded orthogneiss and paragneiss, and younger quartzite and schist. Highly deformed and metamorphosed. Geol. Prov: Paterson orogen.||||||09-JUL-13
26880|Rudall Complex|24535|6|Mentioned|p3 Fig. 1|||Shown as: Palaeoproterozoic igneous and metamorphic rocks.||||||
26880|Rudall Complex|24594|5|Briefly described|p602 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 652+/-5-646+/-11Ma.  Geological Province: Paterson Orogen.  See also p601.||||||07-NOV-08
26880|Rudall Complex|41669|6|Mentioned|p44|||||||||
26880|Rudall Complex|42149|6|Mentioned|p711|||||||||
26880|Rudall Complex|42278|4|Described|p33|||See also Fig.1||||||
26880|Rudall Complex|42702|5|Briefly described|map legend|Proterozoic||||||||
26880|Rudall Complex|42730|4|Described|p16|||||||||
26880|Rudall Complex|42814|6|Mentioned|p16|||||||||
26880|Rudall Complex|43055|6|Mentioned|p26|||||||||
26880|Rudall Complex|43118|4|Described|p8|||see also Table 1.||||||
26880|Rudall Complex|43348|4|Described|P5, Table 1 p6|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
26880|Rudall Complex|43442|6|Mentioned|p12|||Used as a tectonic unit.||||||
26880|Rudall Complex|43561|6|Mentioned|p1436,1440|||||||||
26880|Rudall Complex|43697|5|Briefly described|p25|||Consists of two tectonically interlayered metamorphic sequences: (1) older banded orthogneiss and metasediments of the Yandagooge Formation, and (2) younger quartzite and schist of the Tjingkulatjatjarra Formation.Metamorphosed: approx 1350 Ma.||||||09-JUL-13
26880|Rudall Complex|43756|6|Mentioned|Fig.1,p534|||||||||
26880|Rudall Complex|43847|5|Briefly described|Map Legend||Proterozoic|||||||
26880|Rudall Complex|43848|5|Briefly described|Map Legend||Proterozoic|||||||
26880|Rudall Complex|43849|5|Briefly described|Map Legend||Proterozoic|||||||
26880|Rudall Complex|43856|5|Briefly described|Map Legend||Proterozoic|||||||
26880|Rudall Complex|43867|5|Briefly described|p199, Fig.1 p200|||Same as Rudall Metamorphic Complex.Fig 2||||||
26880|Rudall Complex|44109|5|Briefly described|p165 Fig. 163A|||Geological Province: Paterson Province.  See also p167. ||||||
26880|Rudall Complex|44111|6|Mentioned|p56 Fig.1, p60|||Contains significant mineralisation, including base metals and uranium; also minor PGE and REE.||||||
26880|Rudall Complex|44139|4|Described|p274-278, p280, p282-283|Paleoproterozoic|Paleoproterozoic|Gravity data suggest subsurface link with Wingelina Complex. Northern Paterson Orogen. Unconformably overlain by Coolbro Sandstone, Yeneena Group. Consists of two interlayered metamorphic sequences: older banded orthogneiss and paragneiss, and younger quartzite and schist (Chin et al.  1980). Distribution discussed. Sm-Nd ages of 2250 and 2410 Ma are ~300 - 450 Ma older than inferred crystallisation & suggest contamination by Archean rocks.| | ||||06-MAR-18
26880|Rudall Complex|44866|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
26880|Rudall Complex|49895|6|Mentioned|p2 Fig.1|Proterozoic|Proterozoic|Geological Province: Paterson Orogen.||||||
26880|Rudall Complex|49911|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: 1790-1765Ma.  Geological Province: Paterson Orogen.||||||07-NOV-08
26880|Rudall Complex|50008|4|Described|p43|Paleoproterozoic|Paleoproterozoic|Unconformably overlain by or faulted against the Tarcunyah, Throssell and Lamill Groups. Age of zircon populations given. Geological Province: Paterson Orogen.||||||07-NOV-08
26880|Rudall Complex|50188|6|Mentioned|p10 Fig. 3|||||||||
26880|Rudall Complex|50216|5|Briefly described|p204 Fig.2, p214, 211 Fig.4|||Structural term in this context. Contains granitic gneisses that may represent part of the Dalgaringa Supersuite. Age: 2550-1620 Ma.||||||
26880|Rudall Complex|50219|6|Mentioned|p258 Fig. 1|||Term used in a structural sense.||||||07-FEB-11
26880|Rudall Complex|50222|6|Mentioned|p338|||||||||
26880|Rudall Complex|50228|4|Described|p477, p480 Fig.3|Mesoproterozoic|Paleoproterozoic|Unconformably overlain by the Throssell Group. Consists of multiply deformed sedimentary and igneous rocks. Subdivided into three terranes: Talbot, Connaughton and Tabletop Terranes.||||||07-NOV-08
26880|Rudall Complex|50436|6|Mentioned|p1.1|||||||||
26880|Rudall Complex|50543|5|Briefly described|Map|||Structural term in this context.||||||
26880|Rudall Complex|50620|6|Mentioned|p22|||Structural term in this context.||||||11-AUG-04
26880|Rudall Complex|50621|6|Mentioned|p165 Fig. 6, p167|||Geological Province: Paterson Orogen.||||||
26880|Rudall Complex|60470|5|Briefly described|p3, Fig. 1, p4, p2, 5, 8, 10-11, 15-16|Mesoproterozoic|Paleoproterozoic|Multiply deformed and metamorphosed sedimentary and igneous rocks.  Appears to be used in a 'geological province' sense. Subdivided into >1765 Talbot & Connaughton Terranes and  1465-1222 Tabletop Terrane. Includes quartzite and quartz-muscovite schist. Unconformably overlain by Coolbro Sandstone. Possible source material for Throssell Range and Lamil Group rocks. Hosts Kintyre U mineralization.||||||
26880|Rudall Complex|61154|6|Mentioned|p36|Paleoproterozoic|Paleoproterozoic|Of the Paterson Orogen. Geological Province: Musgrave Block.||||||07-NOV-08
26880|Rudall Complex|61732|6|Mentioned|p83|||Probably a structural term.||||||07-FEB-11
26880|Rudall Complex|62453|5|Briefly described|p4|Paleoproterozoic|Palaoproterozoic|||||||07-NOV-08
26880|Rudall Complex|62986|5|Briefly described|p18|Mesoproterozoic|Paleoproterozoic|Unconformably overlain by the Neoproterozoic Throssell Range Group. Of the Arunta Orogen.||||||07-NOV-08
26880|Rudall Complex|62987|5|Briefly described|p31|||||||||
26880|Rudall Complex|63022|6|Mentioned|p1014 Fig. 1|||Probably structural in this context. ||||||
26880|Rudall Complex|63866|5|Briefly described|p145|||||||||
26880|Rudall Complex|63869|6|Mentioned|p3 Fig.1|||||||||
26880|Rudall Complex|64161|6|Mentioned|p578 Fig.1, p592|Proterozoic|Proterozoic|Igneous and metasedimentary rocks||||||
26880|Rudall Complex|64283|5|Briefly described|p50 Fig. 1, p54 Fig. 4|Paleoproterozoic|Paleoproterozoic|||||||07-FEB-11
26880|Rudall Complex|64635|6|Mentioned|p2 Fig.1|||||||||
26880|Rudall Complex|64722|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|Of the Paterson Orogen.||||||
26880|Rudall Complex|64724|6|Mentioned|p45-46|||Basement to the Neoproterozoic Yeneena Basin||||||02-APR-12
26880|Rudall Complex|64725|5|Briefly described|p74.|Paleoproterozoic|Paleoproterozoic|Hosts the c.800 Ma Kintyre U deposit.||||Is overlain unconformably by Coolbro Sandstone.|Chlorite(-carbonate)-quartz schist, chert.|02-APR-12
26880|Rudall Complex|64726|6|Mentioned|p82.|Paleoproterozoic|Paleoproterozoic|Yapungku Orogeny in this Complex records collision between the West Australian and North Australian Cratons, c.1790 Ma and 1765 Ma.||||||
26880|Rudall Complex|64728|6|Mentioned|p106, p108, p109 Fig.11.|||A possible source of some of the sediment comprising the Bangemall Supergroup.|c.1800 Ma.|||||
26880|Rudall Complex|64733|6|Mentioned|p168, p182|||Of Paterson Orogen.||||||20-APR-12
26880|Rudall Complex|64740|6|Mentioned|p293.|||West Australian Craton.||||||
26880|Rudall Complex|64772|6|Mentioned|p14 Fig.7|||||||||
26880|Rudall Complex|64777|4|Described|p1-3, p6 |Mesoproterozoic|Palaeoproterozoic|Bagas and Smithies (1998) suggested that the earlier deformation had a minimum age of 1760 Ma, based on U-Pb dating of cross-cutting granitic rocks.|1760 Ma|||Unconformably underlies the Throssell Range Group.||
26880|Rudall Complex|64793|6|Mentioned|p282 Fig.1|||||||||
26880|Rudall Complex|64941|5|Briefly described|p27-29|Tonian|Tonian|NW Paterson Orogen. Unconformity-related uranium mineralisation at Kintyre in the Rudall Complex, dated at c 850-840 Ma (Maas and Bagas, in press).|||||Includes chloritic and graphitic schists.|
26880|Rudall Complex|64943|4|Described|p2-5, 6-13,14-15,19,21,22,27,28,33,35|Statherian|Orosirian|Used at Supergroup rank in this report. Composed of paragneiss and orthogneiss, schist and quartzite; a broad imbricate zone of NE- to E-dipping thrust sheets, progressively younger E, deformed and metamorphosed 2015 to 1787-1765 Ma (Yapunku Orogeny).||||||
26880|Rudall Complex|65403|4|Described|p1, pp5-14, pp18-28, Fig.10. |Paleoproterozoic|Paleoproterozoic|This term is restricted to Paleoproterozoic rocks which have been deformed and metamorphosed by the Yapungku Orogeny (c.2000 and 1760 Ma). Situated between the West Australian and North Australian Cratons. Lithologies and metamorphism described in detail. Deposition >1780 Ma. Hosts various (sub-)economic mineral deposits.|1790 +/- 17 to 1765 Ma orthogneiss protolith.|||Unconformably underlies Throssell and Tarcunyah Groups.|Metamorphosed siliciclastic sedimentary rocks and granitoids; amphibolites and mafic granulites; mafic volcanic and intrusive rocks; banded iron-formation, pelite, chert, felsic gneiss; minor quartzite and ultramafic intrusive rocks.|
26880|Rudall Complex|65404|5|Briefly described|p243-265|Paleoproterozoic|Paleoproterozoic|Paterson Orogen. Subjected to Yapungku, Miles and Paterson Orogenies; high-pressure metamorphism c.1790-1760 Ma with a clockwise P-T-t path from at least 40 km of crust thrust over a sequence of basalts and sediments.||||||
26880|Rudall Complex|65416|5|Briefly described|p135, p145.|||Western Officer Basin. Igneous and metamorphic rocks metamorphosed to greenschist facies by Miles Orogeny (1290 - 820 Ma). Post-Cambrian movement saw this unit stepped less to the south than the Musgrave Complex.||||||
26880|Rudall Complex|65454|4|Described|p3-4, p6, p11-13, p22-23, p30-31|Mesoproterozoic|Paleoproterozoic|Multiply deformed supracrustal and intrusive rocks: basement to Paterson area. Includes Fingoon Package. Metamorphosed up to granulite facies. Subdivided into Talbot, Connaughton and Tabletop Terranes. Unconformably overlain by Karara Formation. Contains uranium and base metal mineralisation: over 40 separate prospects.||||||
26880|Rudall Complex|65692|6|Mentioned|p6, p33, p53, p67|||Associated with the 1790-1770 Ma Yapungku Orogeny.||||||
26880|Rudall Complex|65826|5|Briefly described|p2, p3, p5, p7, p9.|Mesoproterozoic|Paleoproterozoic|Includes rocks in the Connaughton, Talbot and Tabletop Terranes. Occurs in the northwestern Paterson Orogen. Consists of multiply deformed and metamorphosed sedimentary and igneous rocks. [Used in a 'geological province' sense.]||||||23-MAY-16
26880|Rudall Complex|65915|6|Mentioned|p2 Fig.1|||||||||
26880|Rudall Complex|66129|6|Mentioned|p224 Fig.12|||||||||
26880|Rudall Complex|66427|6|Mentioned|p74|||Greatly affected by Yapungku Orogeny (1.79-1.76 Ga).||||||
26880|Rudall Complex|66949|6|Mentioned|p91 Appx.5|||Shallow basement on the Wallal Platform.||||||
26880|Rudall Complex|67182|6|Mentioned|p677 Fig.2|Paleoproterozoic|Paleoproterozoic|||||||
26880|Rudall Complex|67195|6|Mentioned|p8|||||||||
26880|Rudall Complex|67202|3|Fully described|p1-6, p16, p22, p33, p41, p43-44, p49-51|Mesoproterozoic|Paleoproterozoic|See also p53-58, p60-64, p66, p73-74, p93-94, p115, p121-125, p127, p134, p136-139, p141, p146, p149-151, p155-156, p159, p161-163, p165, p173, p175, p177, p179, p182-187, p194, p203, p206-207, p219, p221-224, p226, p229, p231, p233, p235, p237-244, p247-249, p254, p256-259, p261-263, p270, p272-273, p277-278, p280-283. Paterson Orogen. Forms uplands and generally has limited outcrop with (semi-) continuous outcrop in the Rudall River National park and Kintyre areas.. Corresponds with high Bouguer anomalies. Gravity and aeromagmetic interpretation; conductivity discussed, imaged and modelled. Upper unconformity is associated with uranium mineralisation. Hosts most U deposits in the Paterson area (eg Kintyre, which is described in detail). Source of uranium and vanadium. Resistivity values. Age of the granite protolith to an augen gneiss. Underwent amphibolite to granulite facies metamorphism in the c.2015-1760 Ma Yapungku Orogeny. Comprises the Talbot, Connaughton and Tabletop Terranes (described). Local silcrete duricrust.|2015 Ma (Hickman and Bagas, 1998).||Yandagooge Formation, Fingoon Quartzite.|Is overlain unconformably by Coolbro Sandstone and Taliwanya Formation (both of the Throssell Range Group) and Tarcunyah Group.|Granulite facies metamorphic rocks including schists, orthogneiss and augen gneiss, BIF, graphitic schist and amphibolite.|15-FEB-18
26880|Rudall Complex|67323|6|Mentioned|p30-31|||Deformed and metamorphosed during the ~1820-1795 Ma Yapungku Orogeny; syn- and post-tectonic granites emplaced ~1790-1765 Ma.||||||
26880|Rudall Complex|67430|6|Mentioned|p1, 3, 22, 69|Paleoproterozoic|Paleoproterozoic|Paterson Province. Hosts the Kintyre U deposit.|||||Carbonaceous metasedimentary rocks.|
26880|Rudall Complex|68055|6|Mentioned|p76 Fig.1|||||||||
26880|Rudall Complex|68902|6|Mentioned|p5-6, p7 fig 4, p10, p20, p25, p27|Mesoproterozoic|Paleoproterozoic|Constitutes the crystalline core of the Paterson Orogen. The Tabletop Terrane of this unit extends underneath the Yeneena Basin, forming a basement high.||||||
26880|Rudall Complex|69091|6|Mentioned|p187|Mesoproterozoic|Paleoproterozoic|Of Paterson Province||||||
26880|Rudall Complex|69417|5|Briefly described|p2:8|||Formed by collision of Western and Northern Australian Cratons.|c.1780 Ma.|||||12-JUL-16
26880|Rudall Complex|72949|6|Mentioned|p33|||Stratigraphic unit or geological province?||||||
26880|Rudall Complex|73184|6|Mentioned|p185 p192, p194-196, p198|||Meta-sedimentary and meta-igneous units contain Archean zircons, and ca 1.80-1.76 Ga Yapungku Orogeny zircons. Possible source of 1.8-1.7 Ga zircons in the Grant Group.|||Tabletop Intrusives [?]||Meta-sedimentary and meta-igneous units including microgneiss.|
23949|Ruins Dolerite|22526|6|Mentioned|Fig3 P682||Orosirian|||||||
23949|Ruins Dolerite|23722|4|Described|p8|Proterozoic|Proterozoic|Formerly Woodward Dolerite. Geological Province: Hooper Complex.||||||06-NOV-15
23949|Ruins Dolerite|42710|5|Briefly described|map legend|Proterozoic||||||||
23949|Ruins Dolerite|42811|4|Described|p6|||age of 1880-1890Ma, of Hooper Complex.||||||
23949|Ruins Dolerite|42814|4|Described|p6|||||||||
23949|Ruins Dolerite|42815|5|Briefly described|map|||||||||
23949|Ruins Dolerite|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
23949|Ruins Dolerite|50437|6|Mentioned|p2.1|||Intrudes Paperbark Supersuite.||||||
23949|Ruins Dolerite|60724|6|Mentioned|p5 Fig. 2, p15|Paleoproterozoic|Paleoproterozoic|Sill intruding the Marboo Formation. Age: 1.88Ga (U-Pb zircon, Page 1991). Within the Hooper Complex. ||||||07-NOV-08
23949|Ruins Dolerite|64580|4|Described|map legend||Paleoproterozoic|Metadolerite.||||||09-DEC-08
23949|Ruins Dolerite|64730|6|Mentioned|p141|Paleoproterozoic|Paleoproterozoic|Intruded Marboo Formation prior to regional deformation.||||Intrudes Marboo Formation.||03-MAY-12
23949|Ruins Dolerite|66846|6|Mentioned|p549 Fig.2|Orosirian|Orosirian|Shown as overlying Marboo Formation. In the Western Zone of the Lamboo Complex.|||||Dolerite sills.|
23949|Ruins Dolerite|68078|6|Mentioned|p7 figure 4|Paleoproterozoic|Paleoproterozoic||~1862 Ma||||Dolerite.|
23949|Ruins Dolerite|69003|6|Mentioned|p5, p19|||W zone, Lamboo Province, Halls Creek Orogen.||||||
23949|Ruins Dolerite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.|||||Coarse- to fine-grained metadolerite; equigranular to porphyritic.|04-AUG-15
23949|Ruins Dolerite|69585|6|Mentioned|p4|Orosirian|Orosirian|Western Lamboo Province.||||||
23949|Ruins Dolerite|69597|6|Mentioned|p5 fig 2b|||||||||
23949|Ruins Dolerite|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone. See 500k_geologyp08_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|1872-1861 Ma (Inferred)||||Coarse- to fine-grained metadolerite; equigranular to porphyritic|
23949|Ruins Dolerite|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Kimberley Craton.|1872 - 1861 Ma.||||Coarse- to fine-grained metadolerite; equigranular to porphyritic.|
23949|Ruins Dolerite|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province; Halls Creek Orogen; North Australian Craton.|||||Coarse- to fine-grained metadolerite; equigranular to porphyritic.|
23949|Ruins Dolerite|70154|5|Briefly described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 250k_interpgeop_lut.csv.|1861-1872 Ma||||Coarse- to fine-grained metadolerite; equigranular to porphyritic.|
23949|Ruins Dolerite|70731|6|Mentioned|p267|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.||||||
23949|Ruins Dolerite|70812|5|Briefly described|p6|Orosirian|Orosirian|Western Zone of the Halls Creek Orogen, Lamboo Province.|c. 1850 Ma||||Mafic magmatics.|
23949|Ruins Dolerite|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|||||||
23949|Ruins Dolerite|70851|5|Briefly described|p3-p4|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province.|c. 1870-1850 Ma|||||
23949|Ruins Dolerite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Metamorphosed at amphibolite grade, and most display large-scale layering of porphyritic and non-porphyritic amphibolite. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyp_lut.csv, 1m_interpgeop_lut.csv and geochron files.|1872-1861 Ma (inferred)|||Intrudes into Marboo Formation.|Medium to fine grained metadolerite forming layered (porphyritic/non-porphyritic) mafic sills, with pods of metaperidotite in places|
23949|Ruins Dolerite|71397|4|Described|p2,5|Orosirian|Orosirian|Geological province: Western Zone, Lamboo Province, Halls Creek Orogen. Commonly metamorphosed to amphibolite facies, and hornfelsed at contact with Marboo Formation; overprinted by layer-parallel foliation during D1/M1 Hooper Orogeny at 1870-1864 Ma (Tyler et al., 1999; Griffin et al., 2000a).  Griffin et al. (1993) identified seven steeply dipping sills with individual units up to 270 m thick.|1872-1861 Ma|||Intrudes into Marboo Formation. Intruded by Paperbark Supersuite.|Metadolerite and metagabbro sills.|
23949|Ruins Dolerite|71873|5|Briefly described|p426,442-443|Orosirian|Orosirian|Geological province: Lamboo Province. Coincides with Rose Bore Granite and Panton Intrusion and Paperbark Supersuite (and Whitewater volcanics), which reflects the suturing of the Western and Central zones during the amphibolite-granulite facies Hooper Orogeny at c. 1860 Ma.|1872-1861 Ma|||Intruded into Marboo Formation.||
23949|Ruins Dolerite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Central Zone, Halls Creek Orogen.|||||Coarse- to fine-grained metadolerite; equigranular to porphyritic.|
23949|Ruins Dolerite|72437|6|Mentioned|p4, p25-26|Palaeoproterozoic|Palaeoproterozoic|Hooper Complex and western zone of the Lamboo Complex. Previously included in the Woodward Dolerite but was renamed by Griffen et al (1993). Described in detail by Derrick and Playford (1973) and Gellatly et al (1974).|c. 1870-1865 Ma|||||
31859|Runton Adamellite|23602|5|Briefly described|p26 Table 4|Mesoproterozoic|Mesoproterozoic|Age: 1080 Ma.||||||
31859|Runton Adamellite|24194|5|Briefly described|p903 Tb.3|Paleoproterozoic|Paleoproterozoic|Parent: Rudall Complex. Geological Province: Paterson Orogeny||||||07-NOV-08
31859|Runton Adamellite|44139|6|Mentioned|p277|Neoproterozoic|Mesoproterozoic|Intrudes Rudall Complex? Rb-Sr age 1080 Ma (Chin & de Laeter, 1981).| | ||||10-SEP-12
31859|Runton Adamellite|50436|5|Briefly described|p1.3, 3.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of the Krackatinny Supersuite.||||||
31859|Runton Adamellite|64943|5|Briefly described|p25 Table 4, p26, p27 Table 5|Neoproterozoic|Mesoproterozoic|1080 Ma by Rb-Sr, post-dates Yeneena Supergroup (Chin and de Laeter 1981); 1067+/-260 Ma by Pb/Pb (Clark and McNaughton, unpubl. data). Monzogranite, non-foliated to weakly foliated. No contacts with Yeneena Supergroup.||||||
27300|Rushall Slate|22715|5|Briefly described|table7 p214|Archean|Archean|Age: 3000-2900Ma.||||||07-NOV-08
27300|Rushall Slate|23244|5|Briefly described|p19,24|||||||||
27300|Rushall Slate|23348|6|Mentioned|220|||||||||
27300|Rushall Slate|23784|4|Described|p24|Archean|Archean|Of Bookingarra Group. Lower part formerly named Comstock Andesite.||||||07-NOV-08
27300|Rushall Slate|23789|5|Briefly described|p18 Tb. 4|Archean|Archean|Of Bookingarra Group.  Max. thickness: 300m.  Geological Province: Pilbara Craton.||||||07-NOV-08
27300|Rushall Slate|23793|4|Described|p23|Archean|Archean|Of Whim Creek Group||||||07-NOV-08
27300|Rushall Slate|23794|5|Briefly described|Map Legend|Archean|Archean|Of Whim Creek Group. Underlying unit Cistern Formation. Geological Province: Pilbara Craton.||||||07-NOV-08
27300|Rushall Slate|23813|5|Briefly described|p90 Tb. 1|Archean|Archean|Of the Bookingarra Group.  Age: 2.965-2.95Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.||||||07-NOV-08
27300|Rushall Slate|23936|5|Briefly described|Tb.1|Archean|Archean|Age: c.3.01-2.99 Ga. Geological Province: Pilbara Craton. Underlying Unit: Cistern Formation.||||||07-NOV-08
27300|Rushall Slate|24023|5|Briefly described|p18|||||||||
27300|Rushall Slate|24140|4|Described|p214 Fig. 1|Archean|Archean|Of Bookingarra Group (reclassified from Whim Creek Group). Volcaniclastic sst, chert and shale. Overlain by Negri Volcanics; overlies Cistern Fm. Min.age: c.2945Ma (Pb model/galena, Houston et al 2000). Max. thickness: 300m.  Geol.Province: Mallina Basin||||||07-NOV-08
27300|Rushall Slate|24184|4|Described|p715|Archean|Archean|Of the Bookingarra Group. Overlies Cistern Formation. Geological Province: Mallina Basin. Age:>2970Ma. Formerly included in Whim Creek Group (Hickman 1983), now assigned to the Bookingarra Group (Smithies et al, 2000)||||||07-NOV-08
27300|Rushall Slate|24185|5|Briefly described|p739 Tb.3|Archean|Archean|Underlain by Cistern Formation. Geological Province: Pilbara Craton.||||||07-NOV-08
27300|Rushall Slate|24191|4|Described|p828 Fig. 1, p830 Fig. 2|Archean|Archean|Of Bookingarra Group.  Overlain by Mount Negri Volcanics; overlies Cistern Fm.  Max. thickness: 300m. Pumaceous sandstone mapped at base (Black, 1999) now correlated with Red Hill Volcanics.  Geological Province: Pilbara Craton.||||||07-NOV-08
27300|Rushall Slate|24192|5|Briefly described|p860|Archean|Archean|Of the Bookingarra Group. Geological Province: Pilbara Craton||||||07-NOV-08
27300|Rushall Slate|24550|5|Briefly described|p36 Tb. 3.2|Archean|Archean|Of the Bookingarra Group. Clastics sediments. Age: 2978Ma.||||||07-FEB-11
27300|Rushall Slate|38498|5|Briefly described|Table 1|||||||||
27300|Rushall Slate|38544|6|Mentioned|Fig.1|||||||||
27300|Rushall Slate|39697|2|Defined|p109|Archean|Archean|||||||07-NOV-08
27300|Rushall Slate|39837|6|Mentioned|Table 1|||||||||
27300|Rushall Slate|41073|6|Mentioned|p206|||||||||
27300|Rushall Slate|41252|6|Mentioned|Table 1|||||||||
27300|Rushall Slate|42231|5|Briefly described|p334|||||||||
27300|Rushall Slate|42973|5|Briefly described|p175|||||||||
27300|Rushall Slate|43595|5|Briefly described|p213|||||||||
27300|Rushall Slate|43698|6|Mentioned|p26|||||||||
27300|Rushall Slate|43769|6|Mentioned|Fig.6,p861|||||||||
27300|Rushall Slate|43821|5|Briefly described|map legend|Archean|Archean|Of Whim Creek Group.||||||07-NOV-08
27300|Rushall Slate|44150|5|Briefly described|p129 Tb.2-15, p132 Fig.2-132, p137|||About 200m thick.||Whim Creek Group||Overlain by Mount Negri Volcanics and Louden Volcanics.|Grey slate and phyllite; a prominent 70m thick andesite unit occurs at Mons Cupri.|
27300|Rushall Slate|61253|5|Briefly described| p52 Fig. 2|Archean|Archean|Age: >2.9 Ga. Geological Province: Pilbara Craton.||||||16-JAN-23
27300|Rushall Slate|63441|5|Briefly described|p5 Tb.1, p27|Archean|Archean|Of Croydon Group (Pilbara Supergroup). Cistern Formation grades up into Rushall Slate;  overlain by Louden and Mount Negri Volcanic Members (of the Bookingarra Formation). Geological province: Mallina Basin, Pilbara Craton.||||||07-FEB-11
27300|Rushall Slate|63538|4|Described|p7, p6 Fig. 3|Archean|Archean|Of Croydon Group. Underlain by Cistern Formation, overlain by Bookingarra Formation. Geological Province: Pilbara Craton.||||||19-APR-13
27300|Rushall Slate|64174|5|Briefly described|Map legend|Archean|Archean|Of the Croydon Group (De Grey Supergroup).  Geological province: Mallina Basin. Metamorphosed shale and siltstone; minor sandstone; graded beds; locally well-developed slatey cleavage.||||||07-NOV-08
27300|Rushall Slate|64580|4|Described|map legend||Mesoarchean|Of Croydon Group. Metamorphosed shale and siltstone; minor sandstone; graded beds; locally well developed slaty cleavage.||||||09-DEC-08
27300|Rushall Slate|65415|5|Briefly described|p119 Fig.1, p121.|Archean|Archean|The lower part of this unit, and the upper part of the underlying Cistern Formation, host the notable massive sulfide mineralisation within the Whim Creek Belt.||Unit in Whim Creek Group.|Includes the Comstock Andesite Member.|Overlies Cistern Formation.||
27300|Rushall Slate|66217|6|Mentioned|p42.|||Mallina Basin.||Unit in Croydon Group.||||
27300|Rushall Slate|67201|4|Described|p7 Fig.4, p12 Tb.1, see comments|||In northwestern Pilbara Craton, West Pilbara Superterrane, De Grey Superbasin. In Whim Creek greenstone belt, with direct lithostratigraphic equivalent within southeastern part of Mallina Basin. Deposited in half-graben sub-basins. Cistern Formation and Rushall Slate represent a continuousy upwards-fining siliciclastic sequence, deposited on uplifted and eroded rocks of Whim Creek Group and later progressed to deep-water distal turbidite deposition in isolated half graben sub-basins, with up to 300 m thick sediment. Page location continued: p21 Fig.12, p23, p57, p60.|c. 2950 Ma|Croydon Group||Gradationally overlies Cistern Formation. Is overlain by (and overlaps with) Bookingarra Formation (Mount Negri Volcanic Member and Louden Volcanic Member).|From Cistern Formation sandstone, passes upward into laminated shale with minor sandstone laminae.|
27300|Rushall Slate|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological Province: Pilbara Craton. [Also assigned to Whim Creek Group in 500k_interpgeop_pilcrat02_lut.csv]. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.||Unit of Croydon Group.|||Metamorphosed shale and siltstone; minor sandstone; graded beds; locally well developed slaty cleavage|
27300|Rushall Slate|69299|5|Briefly described|p6 Tb.1, p7|Archean|Archean|Thickness on COOYA POOYA: 0-300 m. c. 2960 Ma volcanic-hosted massive sulphide Cu-Pb-Zn in Rushall Slate and Cistern Formation on SHERLOCK.||Of Bookingarra Group.|Includes Comstock Member.||Laminated shale and siltstone, locally graphitic, and minor sandstone.|01-JUL-14
27300|Rushall Slate|69300|5|Briefly described|map legend|Archean|Archean|Mallina Basin, Whim Creek greenstone belt.||Bookingarra Group|||metamorphosed well laminated shale and siltstone; minor metasandstone|
27300|Rushall Slate|69301|4|Described|p5 Fig.3, p9 Tb.1, p15|||Pilbara Craton. West Pilbara Superterrane. Mallina Basin.|2950 Ma|Croydon Group||Overlies Cistern Formation. Is overlain by Bookingarra Formation.|Sedimentary rocks. Shale.|
27300|Rushall Slate|70022|6|Mentioned|p115|||West Pilbara Superterrane.||||||
27300|Rushall Slate|70775|5|Briefly described|p12, p41, p43|||Mallina Basin. See also p45-p46, p51, p54-p56, p60, p72, p76, p95-p96.|2955-2948 Ma|Bookingarra Group|Includes the Comstock Member.|Conformably overlies the Cistern Formation. Unconformably overlain by the Louden Volcanics and the Mount Negri Volcanics.||
27300|Rushall Slate|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mallina Basin.|Max age ~2955 Ma, min age 2943+/-7 Ma.|Croydon Group|||Metamorphosed shale and siltstone; minor sandstone; graded beds; locally well developed slaty cleavage.|
27300|Rushall Slate|72251|5|Briefly described|p54|Mesoarchean|Mesoarchean|Geological province: West Pilbara Superterrane, Pilbara Craton.||Unit of Bookingarra Group.||Overlain by Louden or Mount Negri volcanics. Underlain by Cistern Formation. Equivalent to Mallina Formation.||
27300|Rushall Slate|72668|5|Briefly described|p4, p14, p22|||West Pilbara Superterrane.||Croydon Group||Overlies the Cistern Formation. Overlain by the Bookingarra Formation.|Dominantly clastic rocks.|13-JAN-22
41851|Russell Charnockite|67565|2|Defined|p64, p20-21, p6 Table 1, p17, p60, p62.|Statherian|Statherian|New name. Previously included in undifferentiated Arunta Complex (Ranford, 1969) and undifferentiated gneissic granite (Ranford, 1968). Yaya Domain, Warumpi Province. Type locality is northern edge of Ehrenberg Range. Scattered outcrops. Geochemically indistinguishable from, and correlated with, Talyi-Talyi Charnockite. Correlated also with Larrie Granodiorite. Metamorphosed at upper amphibolite facies.||Unit in Waluwiya Suite.||Intrudes Yaya Metamorphic Complex. Is intruded by Ehrenberg Granite and Ilpili Dolerite. Is faulted against the Alkipi Metamorphics.|Distinctive rock type; orthopyroxene- and clinopyroxene-bearing granite, commonly undeformed, with rounded quartz and zoned plagioclase phenocrysts; contains abundant mafic xenoliths; locally foliated with hornblende and leucosomes.|01-DEC-15
41851|Russell Charnockite|69428|5|Briefly described|p13:10-11|Paleoproterozoic|Paleoproterozoic|Close et al. (in prep). Yaya Domain, Warumpi Province. Forms prominent hills at Mount Russell and in the Ehrenberg Range, and scattered small outcrops between the latter and Davenport Hills.||Waluwiya Suite.|||Distinctive rock, commonly undeformed, with abundant rounded plagioclase and pyroxene phenocrysts in a fine-grained granoblastic hornblende-bearing groundmass; abundant mafic xenoliths.|12-JUL-16
41851|Russell Charnockite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||charnockite|
41851|Russell Charnockite|72360|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological province: Warumpi Province. Of Yaya Domain.|||||Charnockite.|09-SEP-19
33889|Ruth Well Formation|22449|5|Briefly described|P25||Archean|||||||07-NOV-08
33889|Ruth Well Formation|22471|6|Mentioned|25|Archean|Archean|Geol province Pilbara||||||07-NOV-08
33889|Ruth Well Formation|23484|4|Described|p10 table 2|Archean|Archean|Of Roebourne Group.||||||07-NOV-08
33889|Ruth Well Formation|23783|5|Briefly described|p37 Tb. 3|Archean|Archean|||||||07-NOV-08
33889|Ruth Well Formation|23784|5|Briefly described|p11|Archean|Archean|Of Roebourne Group.||||||07-NOV-08
33889|Ruth Well Formation|23789|5|Briefly described|p9 Tb. 2|Archean|Archean|Of the Roebourne Group.  Max. thickness: 2000m.  Geological Province: Pilbara Craton.||||||07-NOV-08
33889|Ruth Well Formation|23793|4|Described|p10|Archean|Archean|Of Roebourne Group. Thickness: 2000m.  See also page 12 table 2.||||||07-NOV-08
33889|Ruth Well Formation|23794|5|Briefly described|Map Legend|Archean|Archean|Of Roebourne Group. Geological Province: Pilbara Craton.||||||07-NOV-08
33889|Ruth Well Formation|23813|5|Briefly described|p91 Tb. 1|Archean|Archean|Of the Roebourne Group.  Age: 3.27Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.||||||07-NOV-08
33889|Ruth Well Formation|23936|4|Described|Tb.1|Archean|Archean|Age: 3.27 Ga. Geological Province: Pilbara Craton. Of the  Roebourne Group. Overlain by Nickol River Formation.||||||07-NOV-08
33889|Ruth Well Formation|24023|5|Briefly described|p7 fig. 4|Archean|Archean|Of Roebourne Group. Maximum thickness: 2000m.||||||07-NOV-08
33889|Ruth Well Formation|24024|5|Briefly described|Map Legend|Archean|Archean|Of the Roebourne Group. Geological Province: Pilbara Craton||||||07-NOV-08
33889|Ruth Well Formation|24184|4|Described|p710, p711 Tb.1|Archean|Archean|Of the Roebourne Group. Overlain by Nickol River Formation. Geological Province: Pilbara Craton. Max Thickness: 1-2km. Age: >3270 +/- 2Ma||||||07-NOV-08
33889|Ruth Well Formation|24192|5|Briefly described|p862|Archean|Archean|Geological Province: Pilbara Craton. Komatiitic basalt flows/mafic-ultramafic intrusions, chert and iron-banded formation||||||07-NOV-08
33889|Ruth Well Formation|24541|3|Fully described|p11 Tb.2, p17-18|Archean|Archean|Of the Roebourne Group. Age: undated, but must be older than c. 3270-3250 Ma. Conformably overlain by the Nickol River Formation and intrusive rocks of the Karratha Granodiorite. Maximum thickness: 2000m.||||||07-NOV-08
33889|Ruth Well Formation|24543|5|Briefly described|Map legend|Archean|Archean|Of the Roebourne Group (Pilbara Supergroup).  Metabasalt and serpentiinized preidotite, and thin chert units.||||||07-NOV-08
33889|Ruth Well Formation|24550|5|Briefly described|p36 Tb. 3.2|Archean|Archean|Of the Roebourne Group. Basalt, talc schist, chert. Age: ca 3270Ma. Conformably overlain by Nickol River Formation. Intruded by dykes of the Andover Complex. Max.thickness: 2km. Geological Province: Pilbara Craton. See also p40-41.||||||07-FEB-11
33889|Ruth Well Formation|50430|4|Described|p161||Archean|Mafic to ultramafic formation of Roebourne Group, conformably overlain by Nickol River Formation.||||||07-NOV-08
33889|Ruth Well Formation|61253|5|Briefly described| p52 Fig. 2|Archean|Archean|Age: <3.3 Ga. Geological Province: Pilbara Craton.||||||07-NOV-08
33889|Ruth Well Formation|63441|5|Briefly described|p5 Tb.1, p24|Archean|Archean|Of Roebourne Group. Overlain by Nickol River Fm. Undated. In structural contact with Regal Fm (Regal Terrane). Geol.prov:West Pilbara Superterrane. Includes metabasalt, serpentinised peridotitic komatiite, etc (van Kranendonk 2006).||||||07-FEB-11
33889|Ruth Well Formation|63538|4|Described|p22, p31, p6 Fig. 3|Archean|Archean|Of Roebourne Group. Overlain by Nickol River Formation. Geological Province: Pilbara Craton.||||||19-APR-13
33889|Ruth Well Formation|64174|5|Briefly described|Map legend|Archean|Archean|Of the Roebourne Group. Mafic and ultramafic volcanic and intrusive rocks; minor chert; metamorphosed.||||||07-NOV-08
33889|Ruth Well Formation|64580|4|Described|map legend||Paleoarchean|Of Roebourne Group. Mafic and ultramafic volcanic and intrusive rocks; minor chert; metamorphosed.||||||15-DEC-08
33889|Ruth Well Formation|67201|4|Described|p7, p11, p12 Tb.1, p14, see comments|Archean|Archean|In northwestern Pilbara Craton, Karratha Terrane, West Pilbara Superterrane. Previously included (along with Nickol River Formation) in Roebourne Group. Thickness: up to 2000 m. No stratigraphic base is preserved, lower contacts being either tectonic or intrusive. A hiatus of at least 20 m.y., possibly > 50 m.y. between Ruth Well Formation and Nickol River Formation suggests these Formations should not be assigned to same (Roebourne) Group. Direct dating of Ruth Well Formation is needed to resolve this. Mafic mylonite marks thrust/fault in upper part of unit. Age: > 3270 Ma (intrusion age Karratha Granodiorite); likely < c. 3450 Ma. Related units continued: Harding Granitic Complex occupies core of anticline in Ruth Well Formation. Suggested as analogue of Soanesville Group. Page location continued: p16-17, p25-26, p37, p39-41, p44, p67.|likely < c. 3450 Ma; > 3270 Ma|Roebourne Group||Intruded by Karratha Granodiorite. Overlain by Nickol River Formation separated by mylonite (tectonic contact). Overlain by Andover Intrusion. See comments|Ultramafic and mafic volcanic rocks (peridotite and tholeiitic and komatiitic basalt) with a few thin chert intercalations; metamorphosed. Includes schistose metabasalt, black and dark grey chert, serpentinite and mylonite.|25-NOV-16
33889|Ruth Well Formation|67888|6|Mentioned|p50|Archean|Hadean||>3270 Ma|||||
33889|Ruth Well Formation|68035|4|Described|p289, p290 Fig 5|Paleoarchean||Karratha Terrane, NW Pilbara. Undated. 2 km thick.|>3.20 Ga|||Overlain unconformably by Nickol River Formation.|Metamorphosed ultramafic and mafic volcanic rocks (peridotite to tholeiitic basalt) with a few thin chert intercalations.|
33889|Ruth Well Formation|69185|4|Described|GEOL_LUT_CSV files||Paleoarchean|Geological province: West Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|>3270 Ma|Unit of Roebourne Group.|||Mafic and ultramafic volcanic and intrusive rocks; minor chert; metamorphosed|
33889|Ruth Well Formation|69301|4|Described|p5 Fig.3, p9 Tb.1, p11|||Pilbara Craton. West Pilbara Superterrane. Karratha Terrane. Thickness: 2 km. No stratigraphic base is preserved.|3270 Ma|Roebourne Group||Is overlain by Nickol River Formation. Is intruded by Karratha Granodiorite.|Mafic volcanic rocks. Consists of metamorphosed ultramafic and mafic volcanic rocks (peridotite to tholeiitic basalt) with a few thin chert intercalations.|
33889|Ruth Well Formation|70022|6|Mentioned|p115|||Karratha Terrane, Pilbara Craton.||Roebourne Group.||||
33889|Ruth Well Formation|70775|4|Described|iv, p12, p15, p20-p25|Paleoarchean|Paleoarchean|This formation is a c.1500m thick volcanic succession. Lithology is discussed in some detail. The cooling age of amphibolite facies metamorphism has been interpreted at 3144 +/- 35 Ma by Beintema (2003). Intrusions in this unit have been dated at 3016 +/- 2 Ma and 3017 +/- 6 Ma by Smith (2003). See also p29, p49-p50, p72, p80, p94, p101.|c. 3480-3400 Ma (Nd TDM)|Roebourne Group||Intruded by the Karratha Granodiorite and the Andover Intrusion. Conformably overlain by the Weerianna Basalt.|Komatiite, komatiitic basalt, tholeiite, chert and sills of peridotite and dolerite.|
33889|Ruth Well Formation|72251|5|Briefly described|p54|Paleoarchean|Paleoarchean|Geological province: Karratha Terrane, West Pilbara Superterrane, Pilbara Craton.||Unit of Roebourne Group.||Overlain unconformably by Nicol River Formation.||
33889|Ruth Well Formation|72668|6|Mentioned|p4|||Karratha Terrane of the West Pilbara Superterrane.||Roebourne Group||Overlain by the Nickol River Formation.||
26883|Ryansville Formation|30491|5|Briefly described|p8|||Archaean age||||||
26883|Ryansville Formation|30882|4|Described|p47|||||||||
26883|Ryansville Formation|30960|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
26883|Ryansville Formation|31222|6|Mentioned|p13|||||||||
26883|Ryansville Formation|35269|6|Mentioned|p298|||||||||
26883|Ryansville Formation|36870|3|Fully described|p58|||||||||
26883|Ryansville Formation|38492|5|Briefly described|Table 2|||||||||
26883|Ryansville Formation|38495|6|Mentioned|p18|||||||||
26883|Ryansville Formation|41066|6|Mentioned|1 of 2 N03|||||||||
26883|Ryansville Formation|41841|5|Briefly described|Table 1|||Article recommends abandoning this name use. See p55||||||13-DEC-06
26883|Ryansville Formation|64891|5|Briefly described|p37 Fig. 2, p48-9 Tb. 1|Archean|Archean|Of the Glen Group. Conformably overlain by Wattagee Formation. Age: c.2725Ma. Geological province: Murchison Domain. Thick section of coarse clastic sedimentary rocks, minor chert; weakly metamorphosed.||||||07-FEB-11
26883|Ryansville Formation|65548|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Glen Group, Youanmi Terrane, Yilgarn Craton.Schistose pelite, psammite with porhyroblasts, minor bands of felsic volcaniclastic rock; metachert -locally schistose; basalt -massive to weakly foliated; locally pillowed and/or vesicular; metamorphosed.||||||
26883|Ryansville Formation|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Mapped as four separate but un-named units.|2735 - 2725 Ma.|Unit in Glen Group.|||Chert-pebble to boulder conglomerate; quartz-rich sandstone; siltstone and fine- to coarse-grained sandstone; schistose pelite and psammite, with local biotite porphyroblasts and minor bands of felsic volcaniclastic rock.|
26883|Ryansville Formation|67129|6|Mentioned|p18 fig 19, p38, p39, p41|Archean|Archean|Murchison Domain, Youanmi Terrane.|2735 - 2710 Ma|Glen Group||Unconformably overlies Wilgie Mia Formation|Coarse clastic sedimentary rocks, basal conglomerate, boulder conglomerate, sandstone, pebbly conglomerate.|07-SEP-17
26883|Ryansville Formation|68110|5|Briefly described|p674 Fig. 2|||Murchison Domain.||Of the Glen Group.|||Clastic sedimentary rocks.|
26883|Ryansville Formation|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. Quartzite dated. Conservative estimate of the maximum depositional age from weighted mean 207Pb*/206Pb* zircon date of 2740 +/- 4 Ma.  Age, relationships from Geochron file 185925.1.pdf.||Basal unit of Glen Group.|Includes 6 unnamed units.|Unconformably overlies Wilgie Mia Formation (Polelle Group). Overlain by Wattagee Formation.|Schistose pelite and psammite; Clastic sedimentary rocks; Siltstone and fine- to coarse-grained sandstone; Quartz-rich sandstone; Basalt; Chert pebble to boulder conglomerate; mostly metamorphosed.|23-OCT-15
26883|Ryansville Formation|68698|5|Briefly described|p4-5|Neoarchean|Neoarchean|||Glen Group.||Unconformably overlies Wilgie Mia Formation (Polelle Group). Is overlain conformably by Wattagee Formation.|Clastic sedimentary rocks.|
26883|Ryansville Formation|69583|5|Briefly described|p47, p49, p126; Plate 2|Neoarchean|Neoarchean|Murchison Domain. On p126, "units of the Wattagee Formation are interpreted to underlie [sic] the Ryansville Formation". The Wattagee Formation is also placed below the Ryansville Formation in Plate 2 legend.||Glen Group.||Unconformably overlies Wilgie Mia Formation. Is overlain conformably by Wattagee Formation.|Clastic sedimentary rocks and basalt, with minor chert.|
26883|Ryansville Formation|69584|5|Briefly described|p5 Fig.2|Neoarchean|Neoarchean|||Glen Group||Unconformably overlies the Wilgie Mia Formation, overlain by the Wattagee Formation|Clastic sedimentary rocks.|
26883|Ryansville Formation|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Glen Group.||||
26883|Ryansville Formation|70020|5|Briefly described|p117-118|Neoarchean|Neoarchean|Geological province: Yilgarn Craton. Clastic sedimentary rocks.||Unit of Glen Group.||Overlain by Wattagee Formation. Underlain by Wilgie Mia Formation/Polelle Group.||
26883|Ryansville Formation|70030|5|Briefly described|p192|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton.||Unit of Glen Group.||Lower unit of Glen Group. Overlain by Wattagee Formation. Underlain by Wilgie Mia Formation/Polelle Group.||
26883|Ryansville Formation|70418|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Glen Group.|||Chert pebble to boulder conglomerate, generally well-sorted, weakly metamorphosed; schistose pelite and psammite, local biotite porphyroblasts and minor bands of felsic volcaniclastic rock.|
26883|Ryansville Formation|70796|5|Briefly described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. See also 100K_interpgeop_lut.csv,  500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv,155568.1.pdf, 155572.1.pdf, 185925.1.pdf, 193972.1.pdf, 197420.1.pdf, Cue100_2443_stratig.pdf, Madoonga100_2444_stratig.pdf, MountMagnet100_2441_stratig.pdf. Numerous additional lithologies are discussed.|ca 27352700 Ma (inferred)|Glen Group||Unconformably overlies the Wilgie Mia Formation.|Schistose pelite and psammite; lastic sedimentary rocks; conglomerate, sandstone and siltstone, minor chert; weakly metamorphosed. Siltstone and fine to coarsegrained sandstone; basalt.|
26883|Ryansville Formation|70830|5|Briefly described|p7, p9|||||Glen Group||Conformably overlain by the Wattagee Formation.|Clastic sedimentary rocks.|
26883|Ryansville Formation|71168|4|Described|p7-p8|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c. 2740-2730 Ma|Glen Group||Unconformably overlies the Wilgie Mia Formation (Polelle Group). Overlain by the Wattagee Formation.|Clastic sedimentary rocks.|
26883|Ryansville Formation|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). Sample GSWA 185925 (andalusite-rich quartzite) yielded a weighted mean 207Pb/206Pb date of 2740+\-4 Ma, interpreted to be maximum depositional age of quartzite. Sample GSWA 197420 (quartz metasandstone) yielded a weighted mean 207Pb/206Pb date of 2748+\-5 Ma, interpreted to be maximum depositional age of the metasandstone. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv.|2735-2700 Ma|Unit of Glen Group.||Overlain by Wattagee Formation. Underlain unconformably by Wilgie Mia Formation.|Schistose pelite and psammite; local biotite porphyroblasts, minor bands of felsic volcaniclastics; siltstone, sandstone, chert pebble to boulder conglomerate; metamorphosed; basalt, massive to foliated, locally pillowed, vesicular, metamorphosed|
26883|Ryansville Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Youanmi Terrane.|||||Clastic sedimentary rocks; conglomerate, sandstone and siltstone; minor chert; weakly metamorphosed.|
26883|Ryansville Formation|73410|5|Briefly described|p2, 13|||Youanmi Terrane. Mapped with Marda Formation.|c.2730 Ma.|Glen Group.|||Greenstone; metaconglomerate, metasandstone and felsic volcanics.|
26883|Ryansville Formation|73596|6|Mentioned|p1160, 1165, 1170|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. Conglomerate clasts derived from underlying Polelle Group (eg BIFs from Wilgie Mia Formation).|2734 +/- 5 Ma (MDA) - 2716 +/- 4 Ma (min).|Glen Group.|||Clastic sedimentary rocks: basal conglomerate overlain by gritstone, sandstone and shale, interlayered with felsic volcanic rocks and tuffs.|
27229|Sadler Limestone|22550|6|Mentioned|Fig 3|||||||||
27229|Sadler Limestone|22741|5|Briefly described|P21, P23, Table3 P17|Givetian|Frasnian|Equivalent to Gogo Formation.||||||13-NOV-07
27229|Sadler Limestone|23903|5|Briefly described|p1595, p1597 Fig.2|Frasnian|Givetian|Geological Province: Canning Basin.||||||13-NOV-07
27229|Sadler Limestone|24000|5|Briefly described|p348|Devonian|Devonian|Geological Province: Canning Basin.||||||
27229|Sadler Limestone|24061|5|Briefly described|p180|Middle Devonian|Middle Devonian|Of "Lennard River Group"?  Geological Province: Canning Basin.||||||28-MAY-08
27229|Sadler Limestone|30181|6|Mentioned|Fig.75|||||||||
27229|Sadler Limestone|30187|6|Mentioned|p179|||||||||
27229|Sadler Limestone|31150|6|Mentioned|p96|||Forereef facies||||||
27229|Sadler Limestone|31151|6|Mentioned|p68|||||||||
27229|Sadler Limestone|31152|6|Mentioned|p2|||||||||
27229|Sadler Limestone|31332|6|Mentioned|Fig. 3|||||||||
27229|Sadler Limestone|31661|6|Mentioned|p666|||M.Devonian||||||
27229|Sadler Limestone|31870|6|Mentioned|p9|||||||||
27229|Sadler Limestone|32619|6|Mentioned|p464|||Givetian||||||
27229|Sadler Limestone|32647|6|Mentioned|Fig. 24|||||||||
27229|Sadler Limestone|32865|6|Mentioned|p471|||See also P472-473. Frasnian||||||
27229|Sadler Limestone|33042|6|Mentioned|p743|||Frasnian. See also PP744-753 & Figs & plates||||||
27229|Sadler Limestone|33112|6|Mentioned|p179|||||||||
27229|Sadler Limestone|34427|6|Mentioned|Fig.3|||||||||
27229|Sadler Limestone|34428|6|Mentioned|p1009|||||||||
27229|Sadler Limestone|35104|6|Mentioned|p5|||||||||
27229|Sadler Limestone|36225|6|Mentioned|Map legend|Frasnian|Givetian|Givetian to Frasnian||||||
27229|Sadler Limestone|36257|6|Mentioned|Table 2.1|||||||||
27229|Sadler Limestone|36365|6|Mentioned|Fig.8|||||||||
27229|Sadler Limestone|36743|6|Mentioned|p42|||||||||
27229|Sadler Limestone|36890|3|Fully described|p333|||Formerly Sadler Formation.||||||10-NOV-08
27229|Sadler Limestone|38207|6|Mentioned|Fig.1|||||||||
27229|Sadler Limestone|39702|6|Mentioned|Fig.2|||||||||
27229|Sadler Limestone|40793|6|Mentioned|Fig.3|||||||||
27229|Sadler Limestone|40797|6|Mentioned|p155|||||||||
27229|Sadler Limestone|40866|6|Mentioned|p179|||||||||
27229|Sadler Limestone|41139|6|Mentioned|Fig.2|||||||||
27229|Sadler Limestone|41512|6|Mentioned|p30|||||||||
27229|Sadler Limestone|41894|4|Described|p4|||||||||
27229|Sadler Limestone|42030|5|Briefly described|p747|||||||||
27229|Sadler Limestone|42073|6|Mentioned|Fig.2 P292|||||||||
27229|Sadler Limestone|42080|6|Mentioned|p281|||||||||
27229|Sadler Limestone|42111|5|Briefly described|p88|||See also Text fig.4||||||
27229|Sadler Limestone|42176|6|Mentioned|Fig.2 P204|||||||||
27229|Sadler Limestone|42347|6|Mentioned|Fig.2 P1020|||||||||
27229|Sadler Limestone|42351|5|Briefly described|Fig.4 P41|||||||||
27229|Sadler Limestone|42564|5|Briefly described|p9|||||||||
27229|Sadler Limestone|42860|5|Briefly described|Fig.2|||||||||
27229|Sadler Limestone|42880|5|Briefly described|Fig.2,p1020|||||||||
27229|Sadler Limestone|42930|5|Briefly described|Fig.1 p473|Devonian|Devonian|Interfingers with Gogo Shale, Pillara Limestone and Virgin Hills Formation. Geological Province: Canning Basin.||||||13-NOV-07
27229|Sadler Limestone|42933|5|Briefly described|Fig.94 p258|||||||||
27229|Sadler Limestone|43173|6|Mentioned|54||Late Devonian|||||||
27229|Sadler Limestone|43563|6|Mentioned|Fig.5,p10|Late Devonian|Middle Devonian|||||||
27229|Sadler Limestone|43723|6|Mentioned|p51||Devonian|||||||
27229|Sadler Limestone|44143|4|Described|p438 Table 4-19, p442, p443 Figure 4-98|Devonian|Devonian|Up to 350m thick; calcarenite & calcirudite; shallow marine. Interfingers with Pillara Limestone and Gogo Formation. Type section in Emanuel Range (NOONKANBAH: 18deg 36' S, 125deg 56' E). Contains brachiopods, ammonoids, conodonts, corals and algae; late Givetian to Frasnian.||||||24-NOV-17
27229|Sadler Limestone|44231|5|Briefly described|Map Legend|Frasnian|Givetian|Fore-reef subfacies; calcarenite and limestone breccia and megabreccia. Geological Province: Canning Basin.||||||26-MAY-05
27229|Sadler Limestone|44397|14|Not recorded|p.12, Figs.2,3,Tb.4|||Frasnian to (?) Givetian.||||||
27229|Sadler Limestone|44398|14|Not recorded|map legend|||Frasnian to Givetian.||||||
27229|Sadler Limestone|45039|6|Mentioned|Fig.5|||||||||
27229|Sadler Limestone|45063|6|Mentioned|Fig. 9|||Devonian||||||
27229|Sadler Limestone|45101|4|Described|p6|||Conodont content.||||||10-NOV-08
27229|Sadler Limestone|45153|2|Defined|App.3-51|Late Devonian|Late Devonian|||||||
27229|Sadler Limestone|45158|3|Fully described|p26|||||||||
27229|Sadler Limestone|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
27229|Sadler Limestone|47039|6|Mentioned|p133|||||||||
27229|Sadler Limestone|60333|5|Briefly described|p802|Devonian|Devonian|Marginal slope facies. Geological Province: Canning Basin.||||||
27229|Sadler Limestone|62735|5|Briefly described|p982|Frasnian|Frasnian|A steep forereef facies. Overlies Pillara Formation. Geological Province: Canning Basin.||||||04-OCT-06
27229|Sadler Limestone|63938|5|Briefly described|p49 Fig.1, p50 fig.2|Frasnian|Givetian|Marginal slope.||||||10-NOV-08
27229|Sadler Limestone|64159|5|Briefly described|p91 Fig. 6|Frasnian|Givetian|Part of the Lennard Reef facies development.||||||
27229|Sadler Limestone|64502|6|Mentioned|p767|||Misspelling of Sadler Formation?||||||10-NOV-08
27229|Sadler Limestone|64580|5|Briefly described|map legend|||Givetian-Frasnian reef complexes, marginal slope and basin facies.||||||15-DEC-08
27229|Sadler Limestone|64643|5|Briefly described|p5 Fig. 4, p7 Fig.5, p34, 35|Frasnian|Givetian|Marginal slope facies.||||||24-NOV-08
27229|Sadler Limestone|64783|6|Mentioned|p101|||Canning Basin.||||||15-NOV-17
27229|Sadler Limestone|65214|6|Mentioned|p280|Devonian|Devonian|Canning Basin. Appears as Sadler Formation on p277. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
27229|Sadler Limestone|65486|5|Briefly described|p6-70, Plate 1.|Frasnian|Givetian|Marginal-slope and basin limestone, siltstone, and shale, Canning Basin. Also referred to as Sadler Formation. Overlies Pillara Limestone and Cadjebut Formation. Underlies and interfingers with Gogo Formation. Underlies Napier and Virgin Hills Formations.||||||
27229|Sadler Limestone|66127|3|Fully described|pp19-21, p49-51, p177-189, p199-202|Frasnian|Givetian|Of Playford and Lowry (1966); formerly Sadler Formation of Guppy et al.(1958); name changed to reflect the dominant and characteristic lithology. Exposed at Sadler Ridge and along north side of the Emanuel Range. Richly fossiliferous; silicified fossils, especially brachiopods, very common on weathered surfaces. Thickness to 700 m. Shown on Plates 3, 4, 5, 7, 8.||||Abuts and interfingers with Pillara Limestone and Gogo Formation. Is overlain by Virgin Hills Formation.|Marginal-slope and basin facies: grey, thick- to thin-bedded limestone; contains scattered allochthonous blocks of reef limestone, some debris-flow deposits, and common silicified fossils. Fore-reef subfacies has abundant breccia.|
27229|Sadler Limestone|67131|6|Mentioned|p3 Fig. 2,|Frasnian|Givetian|Marginal slope facies.||||Overlain by Virgin Hills Formation.||
27229|Sadler Limestone|69099|6|Mentioned|500k_geologyp08_lut.csv|Frasnian|Givetian|Givetian-Frasnian reef complexes, marginal slope and basin facies. Grouped as Sadler Limestone, Gogo Formation, lower Virgin Hills Formation, and lower Napier Formation in 500k_geologyp08_lut.csv.||||||04-AUG-15
27229|Sadler Limestone|69165|6|Mentioned|500k_geologyp08_lut.csv|Frasnian|Givetian|||||||
27229|Sadler Limestone|69182|6|Mentioned|Ch4 p39, Ch4 p87|||||||||
27229|Sadler Limestone|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Fossiliferous, shallow marine reef complex marginal slope facies yellow to light grey calcarenite and calcirudite with thinner beds of calcareous siltstone and shale; slump folding is common, with rolled blocks of reef limestone in places|
27229|Sadler Limestone|72489|6|Mentioned|p13 Fig.10|||Only shown on p13 Fig.10. Temporal relationships diagram.||||||
27229|Sadler Limestone|72502|6|Mentioned|p5|Frasnian|Givetian|Lennard Shelf, Canning Basin.||||Underlain by Cadjebut Formation. Overlain by Virgin Hills Formation. Equivalent to Gogo Formation and Pillara Limestone.||
34609|Saffron Sandstone|22702|4|Described|p104,106-8,112-3||Barremian|||||||
34609|Saffron Sandstone|60379|6|Mentioned|p132|||||||In part equivalent to Muderong Shale?||
23950|Sahara Formation|14228|5|Briefly described|p6 fig3, p15|Late Silurian|Early Silurian|South Canning Basin.||Carribuddy Group||||06-OCT-16
23950|Sahara Formation|22753|5|Briefly described|Fig.3 p585|Silurian|Silurian|||||||
23950|Sahara Formation|24449|5|Briefly described|p741 Fig. 2|Wenlockian|Llandoverian|Of Carribuddy Group.  Age: ~425m.y.  Geological Province: Canning Basin.||||||
23950|Sahara Formation|40837|2|Defined|p257 Fig. 4, p273|Emsian|Emsian|Of the Carribuddy Group - replacing Unit A of Carribuddy Formation. See also Fig. 5 page insert (p258).||||||27-JAN-10
23950|Sahara Formation|42030|6|Mentioned|p746|||||||||
23950|Sahara Formation|43563|6|Mentioned|Fig.2, p4-5|||||||||
23950|Sahara Formation|43599|6|Mentioned|p250, Fig.3||Silurian|||||||
23950|Sahara Formation|43656|6|Mentioned|Fig.2,p8|Pridoli|Llandovery|||||||
23950|Sahara Formation|43666|6|Mentioned|p20||Silurian|||||||
23950|Sahara Formation|43746|6|Mentioned|Fig.2,p11|Pridoli|Ashgillian|||||||
23950|Sahara Formation|44143|4|Described|p.440 Table 4-19; p.442, Figure 4-96|Devonian|Silurian|Unit in Carribuddy Group. Up to 279m thick; red-brown dolomite and siltstone; sabkha & supratidal marine. Conformably overlies Mallowa Salt. Type section between 2,688 and 2,967m in Kidson 1 (URAL: 22deg 37' 27" S, 125deg 00' 17" E). Contains sparse spores and pollen.||||||
23950|Sahara Formation|61551|6|Mentioned|p351 Fig.2. |Pridoli|Ruddanian|||||Overlies Mallowa Salt.||
23950|Sahara Formation|64334|5|Briefly described|p39|Silurian|Silurian|Canning Basin; subsurface only. Llandovery.||Carribuddy Group.||Overlies Nibil Formation and Mallowa Salt.|Mudstone.|
23950|Sahara Formation|64643|5|Briefly described|p3 Fig. 2|Llandovery||Of Carribuddy Group?||||||
23950|Sahara Formation|64982|5|Briefly described|p699 Fig.4.|Llandovery|Llandovery|Up to 140 m thick supratidal deposits. Sparse spores and pollen but no reliable age dating.||Unit in Carribuddy Group.||Overlies Mallowa Salt.|Red-brown dolomite and siltstone.|
23950|Sahara Formation|65301|5|Briefly described|p5 Fig. 4, p8 Fig. 5|Llandovery|Llandovery|Geological province: Canning Basin.||||||
23950|Sahara Formation|65449|4|Described|p1, p6-9, p11, p13-14, p23,p27-29,p31-33|Llandovery|Late Ordovician|See also p40, p47-50, p54-57; Plates 1-9, 11. Lehmann (1984), after Sahara 1 well where it was first encountered. Type section is the interval 2967-2688m in Kidson 1. Up to 280m thick; average thickness is c.130m. Age range from surrounding units.||Carribuddy Group.|Pegasus Dolomite Member.|Overlies Mallowa Salt (diachronous). Is overlain conformably by Dodonea Member (Worral Formation).|Dominantly red-brown argillaceous, silty and sandy dolomite grading to dolomitic mudstone, with minor sandstone interbeds; anhydrite is common throughout as small nodules and vein fillings. Pale green reduction spots.|
23950|Sahara Formation|68007|6|Mentioned|p4, p11, Plate 1|Silurian|Silurian|Canning Basin.|||Pegasus Dolomite Member.|Overlies Mallowa Salt. Is overlain by Worral Formation.||
23950|Sahara Formation|68902|5|Briefly described|p9 fig 5|Silurian|Silurian|||Carribuddy Group||Overlies Mallowa Salt and Nibil Formation; overlain by Worral Formation.||
23950|Sahara Formation|69029|6|Mentioned|p319|Silurian|Silurian|Of Canning Basin.||||Overlain by Worral Formation. Underlain by Mallawo Salt.||
23950|Sahara Formation|69182|6|Mentioned|Ch4 p9-p12, Ch4 p44|Llandovery|Llandovery|Canning Basin. See also Ch4 p45, Ch4 p47, Ch4 p50-p58, Ch4 p74, Ch4 p79-p82. ||Carribuddy Group||Overlies the Mallowa Salt and the Nibil Formation.|Sandstones and dolomites.|
23950|Sahara Formation|69312|6|Mentioned|p3, p19, p23 fig 26|Llandovery|Llandovery|Canning Basin. See also  p24 fig 28, p25 fig 30, p26 fig 32, p27 fig 34, p28 fig 36. ||Carribuddy Group||Overlies the Mallowa Salt. Overlain by the Worral Formation or the Tandalgoo Sandstone.|Shale.|
23950|Sahara Formation|69883|5|Briefly described|p4-p6|Pridoli|Llandovery|Canning Basin. Supersequences provided. Conodonts indicate some marine influence. Contains age-diagnostic fossils in the form of Early Silurian conodonts. Contains potential petroleum source rocks.||Carribuddy Group||Overlies the Mallowa Salt.||26-FEB-20
23950|Sahara Formation|70774|5|Briefly described|p4|Llandovery|Llandovery|Willara and Kidson Sub-basins, Canning Basin.||Carribuddy Group||Overlies the Mallowa Salt. Overlain by the Worral Formation.||
23950|Sahara Formation|71171|6|Mentioned|p2|||Canning Basin.||||||
23950|Sahara Formation|71870|5|Briefly described|p3|Pridoli|Rhuddanian|Canning Basin.||Carribuddy Group||Overlies the Mallawa Salt. Unconformably overlain by the Worral Formation and Tandalgoo Sandstone.||
23950|Sahara Formation|71894|5|Briefly described|p4|Llandovery|Llandovery|Canning Basin.||Carribuddy Group||Overlies the Mallowa Salt. Overlain by the Worral Formation.|Shale.|
23950|Sahara Formation|72497|5|Briefly described|p3 Fig.2.|Pridoli|Katian|Shown as occuring in the Anketell, Tabletop, Ryan Shelves, Willara and Kidson Sub-basins, the Jurgurra and Barbwire Terraces and Broome Platform. Age shown as Ashgillian to Pridolian ~=Bolindian- Pridoli (Aust), Katian - Pridoli (ICS).||Carribuddy Group||Conformably overlies Mallowa Salt. Unconformably overlain by Tandalgoo Formation.||
23950|Sahara Formation|72499|5|Briefly described|p7 Fig.6.|Llandovery|Llandovery|Located in the Willara Sub-basin and Broome Platform.||||Overlies Mallowa Salt ?and Nibil Formation. Underlies Worral Formation.|Includes shale.|
23950|Sahara Formation|73117|5|Briefly described|p3|Llandovery|Llandovery|Canning Basin.||Carribuddy Group||Underlain by Mallowa Salt. Overlain by Worral Formation.|Dominantly shale and mudstone.|
23950|Sahara Formation|73344|6|Mentioned|p6|Pridoli|Rhuddanian|Canning Basin, subsurface. Part of supersequence B2.||Carribuddy Group||Underlain by Mallowa Salt.||
68076|Salisbury Gneiss|24526|5|Briefly described|p105 Fig. 6, p108-109|Mesoproterozoic|Mesoproterozoic|Of the Nornalup Complex.  Comprises garnet-cordierite migmatite and mafic granulite.  Age: ~1215Ma.  Part of the Albany-Fraser Orogen.  See also p106 Fog. 7.||||||
68076|Salisbury Gneiss|62381|5|Briefly described|p2 Fig.2, p3 Fig.3.|||Metamorphosed 1214 +/- 8 Ma (peak) and 1182 +/- 13 Ma (thrusts).||Unit in Nornalup Complex.||Thrust over Nornalup Complex at c.1180-1170 Ma.|Garnet-cordierite migmatite and mafic granulite.|03-JUL-14
68076|Salisbury Gneiss|63866|5|Briefly described|p183, p191, p198|||Outcrops on a series of islands at the southeast margin of the Nornalup Complex.|c. 1215 Ma||||Garnet-cordierite migmatite and mafic granulite.|
68076|Salisbury Gneiss|64722|6|Mentioned|Fig. 8 p18|||Possibly the same as Salisbury metasedimentary rocks, p28?||||||
68076|Salisbury Gneiss|65487|4|Described|p24, 51-52, 59, p56-57 Fig. 27|Mesoproterozoic|Mesoproterozoic|Protoliths deposited between Stage 1 and Stage II tectonism (ie c.1260-1215 Ma). Interpreted as cover rocks overlying the Nornalup Zone. Pelitic gneisses and mafic granulite, porphyritic granitic gneiss and two-pyroxene metagabbro. Separated from the Malcolm Gneiss by the Rodona Fault.||||||
68076|Salisbury Gneiss|67268|6|Mentioned|p9, p16, p19|Mesoproterozoic|Mesoproterozoic|Nornalup zone. Underwent granulite facies metamorphism at approximately 1214 +/- 8 Ma. ||||||
68076|Salisbury Gneiss|67380|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|||||||
68076|Salisbury Gneiss|67722|5|Briefly described|p1,p5 p12, p17, p20, p90, p97|Mesoproterozoic|Mesoproterozoic|Nornalup Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen. Granulite facies metamorphism  at 1214+/-8 Ma, exhumation at 1182 +/-13 Ma|||||Deformed granulite facies metapelitic gneiss with subordinate granite, felsic and mafic gneisses.|
68076|Salisbury Gneiss|68186|4|Described|p8, p28-30, p40-41|Mesoproterozoic|Mesoproterozoic|Crops out on islands SE of Esperance. Although situated within the Madura Province, it is inferred to be part of the Ragged Basin. Cover unit overlying Nornalup Zone, Kepa Kurl Booya Province. Pelitic protoliths, sourced from the Recherche Supersuite and deposited in shallow intracratonic basins. An age determination of 1182 +/- 13 Ma reflects zircon rim growth after peak metamorphic conditions.|1214+/-8 Ma (crystallisation: Clark et al.,2000)|||Faulted against Malcolm Metamorphics.|Pelitic gneisses and mafic granulite, porphyritic granitic gneiss, and a two-pyroxene metagabbro deformed only at its margins. Also migmatitic pelitic gneiss with K-feldspar-rich leucosomes (dated).|
68076|Salisbury Gneiss|68654|6|Mentioned|p3|Mesoproterozoic|Mesoproterozoic|Ragged Basin, Albany-Fraser Orogen.|<1260 Ma|||||
68076|Salisbury Gneiss|69003|5|Briefly described|p43-44|||Madura Province. No detrital zircon geochronology, but sedimentary protoliths were probably deposited around 1260-1225 Ma. Underwent high-T metamorphism and deformation in the period 1225-1140 Ma.||||||
68076|Salisbury Gneiss|69252|5|Briefly described|p2, p9, p16-17, p21-22, p24, p76|Mesoproterozoic|Mesoproterozoic|Clark et al. (2000). Ragged Basin. Nornalup Zone, Albany-Fraser Orogen. Named after Salisbury Island, one of an isolated series of islands 165km SE of Esperance. Geochronologically different from Malcolm Metamorphics. Protolith sediments were derived from Albany-Fraser Orogen. Metamorphism (1214 Ma - 1182 Ma) described.|1260-1215 Ma (protolith deposition age).||||Metapelitic gneisses and mafic granulite, with subordinate porphyritic granite-gneiss and two-pyroxene metagabbro.|
68076|Salisbury Gneiss|69595|5|Briefly described|p26, p27|||Madura Province. |1214 +/- 8 Ma (minimum depositional age)||||Pelitic gneisses and mafic granulite, porphyritic granitic gneiss anda  two-pyroxene metagabbro that is undeformed in its core but deformed and amphibolitic at its margins.|
68076|Salisbury Gneiss|70023|4|Described|p168-169,184-185|||Geological province: Madura province; Albany-Fraser Orogen. Potentially emplaced during uplift and erosion of Norlanup Zone between Stages I and II Albany-Fraser Orogen. Includes a metasedimentary component, and found on isolated islands ~165km SE of Esperance (Clark et al., 2000). Overthrusting of Salisbury Gneiss olong Rodona Shear Zone at c. 1154 during Stage II Albany-Fraser Orogeny via deztral shearing and NW-SE thrussting and crustal thickening (Clark et al., 2000). U-Pb zircon rims analysis from a migmatitic leucosome yielded 1182+\-13 Ma age, interpreted to represent growth during post-peak decompression melting (Clark et al., 2000).||||||
68076|Salisbury Gneiss|70182|6|Mentioned|p3|||Albany-Fraser Orogen.||||||
68076|Salisbury Gneiss|70802|5|Briefly described|500k_interpgeop14_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen. Of Barren Basin. Events: Albany-Fraser Orogeny Stage II (1225-1140 Ma).|1320 Ma (inferred); 1214+\-8 Ma ||||Pelitic gneiss and mafic granulite; porphyritic granitic gneiss and metagabbro|
68076|Salisbury Gneiss|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Ragged Basin, Albany-Fraser Orogen.|Max age ~1320 Ma, Min age 1214+/-8 Ma.||||Pelitic gneiss and mafic granulite; porphyritic granitic gneiss and metagabbro.|
68076|Salisbury Gneiss|73084|6|Mentioned|p12|||Madura Province.||||||
31785|Sally Downs Supersuite|22716|5|Briefly described|p232|Orosirian|Orosirian|Part of the Bow River Batholith.||||||
31785|Sally Downs Supersuite|23323|5|Briefly described|p454 Fig.2|Orosirian|Orosirian|Age: 1830-1800 Ma.||||||07-FEB-07
31785|Sally Downs Supersuite|23383|5|Briefly described|p6 Fig 3|Paleoproterozoic|Paleoproterozoic|Elsewhere referred to as Sally Downs supersuite.  Age 1835-1805 Ma.||||||07-NOV-08
31785|Sally Downs Supersuite|23622|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Bow River Batholith.||||||07-NOV-08
31785|Sally Downs Supersuite|23925|5|Briefly described|p222 Table 3|||Geological Province: Halls Creek Orogen.||||||
31785|Sally Downs Supersuite|24197|4|Described|p20|Paleoproterozoic|Paleoproterozoic|Example of Sally Downs Assocn. Type example is Sally Downs Suite. Contains the plutons: Mabel Downs and Sally Downs Tonalite, McHale Granodiorite, Corrara, Mount Fairbairn and Shepherds Bore Granites, and Grimpy Monzogranite. In east Kimberley region.||||||07-FEB-11
31785|Sally Downs Supersuite|43855|5|Briefly described|Map Legend||Proterozoic|||||||
31785|Sally Downs Supersuite|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Age: 1825Ma. Geological Province: Kimberley Region.||||||07-NOV-08
31785|Sally Downs Supersuite|60533|5|Briefly described|p593|Paleoproterozoic|Paleoproterozoic|Age: ca. 1835Ma. Geological Province: Halls Creek Orogen.||||||07-NOV-08
31785|Sally Downs Supersuite|61861|6|Mentioned|Fig.2.|||Halls Creek, eastern zone.|1830-1800 Ma.|||||
31785|Sally Downs Supersuite|63866|5|Briefly described|p128-p132, p138|||Central Zone, Halls Creek Orogen.|1835-1808 Ma||Includes the Mount Christine Granitoid, Mabel Downs Tonalite, McHale Granodiorite, Loadstone monzogranite, Sally Downs Tonalite, Copperhead Carbonatite and the Eastman Granite.|||
31785|Sally Downs Supersuite|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Mafic intrusions; biotite-bearing norite, gabbronorite, gabbro; cut by veins of granitoid rock; Fine- to coarse-grained biotite monzogranite, syenogranite, and granodiorite; biotite(-hornblende) tonalite; even-textured to porphyritic.||||||15-DEC-08
31785|Sally Downs Supersuite|68078|6|Mentioned|p4 figure 2, p23|Paleoproterozoic|Paleoproterozoic||1835 - 1805 Ma||||Granites.|
31785|Sally Downs Supersuite|68656|5|Briefly described|GEOL_LUT_CSV/500k_geologyp08_lut|Paleoproterozoic|Paleoproterozoic||||||Granitic intrusions: fine- to coarse-grained biotite monzogranite, syenogranite, and granodiorite; biotite(-hornblende) tonalite. Mafic intrusions; biotite-bearing norite, gabbronorite, gabbro, and tonalite with veins of intermediate hybrid rock.|
31785|Sally Downs Supersuite|69003|5|Briefly described|p5, p18-20|Paleoproterozoic|Paleoproterozoic|Central zone, Lamboo Province, Halls Creek Orogen.|1835-1805 Ma.||||Voluminous granites.|
31785|Sally Downs Supersuite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.|||Includes Wild Dog Creek Gabbro, Emull Gabbro, Kevins Dam Suite, McIntosh Suite, Syenite Camp Suite, Mabel Downs Suite and 6 unnamed units||Granite, monzogranite, syenogranite, and granodiorite, gabbro, and layered mafic-ultramafic intrusions; lesser metasedimentary hornfels.|04-AUG-15
31785|Sally Downs Supersuite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_geologyp08_lut.csv. |||Includes Kevins Dam Suite, McIntosh Suite, Syenite Camp Suite, Mabel Downs Suite, Wild Dog Creek Gabbro, Emull Gabbro||Undivided; granite, gabbro and layered mafic-ultramafic intrusions, equigranular biotite monzogranite. Medium- coarse grained, porphyritic biotite monzogranite, syenogranite and granodiorite. Biotite norite, olivine gabbronorite, gabbronorite.|
31785|Sally Downs Supersuite|69585|5|Briefly described|p3-5, p31|Orosirian|Orosirian|Associated with Halls Creek Orogeny. These granitic rocks stitched the western, central and eastern zones of the Lamboo Province. Is considerably more juvenile than the older Paperbark Supersuite, implying a higher degree of mantle melting.|1835-1805 Ma.||||Adakites, calc-alkaline and high-K calc-alkaline granites, high-K monzogranite and syenogranite.|
31785|Sally Downs Supersuite|69587|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Plutonic granitic intrusions; fine- to coarse-grained biotite monzogranite, syenogranite, and granodiorite; biotite(-hornblende) tonalite; even-textured to porphyritic|
31785|Sally Downs Supersuite|69597|6|Mentioned|p3, p4, p5 fig 2b|||Intrudes the Central and Eastern zones of the Lamboo Province. |1835-1805 Ma|||||
31785|Sally Downs Supersuite|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|1832-1808 Ma (Isotopic)||Includes Syenite Camp Suite, Kevins Dam Suite, Emull Gabbro, Wild Dog Creek Gabbro.||Biotite-bearing norite, olivine gabbronorite, gabbronorite, gabbro, quartz gabbro, dolerite, leucogabbro with veins of intermediate hybrid rock; cut by abundant veins of coarse-grained porphyritic granite; layered mafic-ultramafic intrusions|
31785|Sally Downs Supersuite|70154|4|Described|100k_interpgeol_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|1808-1832 Ma||Wild Dog Creek Gabbro, Kevins Dam Suite, Emull Gabbro, McIntosh Suite, Syenite Camp Suite, Mabel Downs Suite||Granite, gabbro and layered mafic-ultramafic intrusions.Medium-coarse grained porphyritic biotite monzogranite, syenogranite and granodiorite. Granitic and gabbroic rocks. Norite, olivine bearing gabbronorite and quartz gabbro.|
31785|Sally Downs Supersuite|70731|5|Briefly described|p268-270,272-273,276-278|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. Voluminous felsic and mafic magmatism in the central Lamboo Province during Halls Creek Oregeny. Nd isotopic data show proportion of mantle-derived material. Mostly undeformed/unmetamorphosed, but in contact with with granulite-facies Tickalara Metamorphics.|1835-1805 Ma|||||
31785|Sally Downs Supersuite|70812|5|Briefly described|p5-p6, p8-p9, p20, p24-p25, p27-p29|Orosirian|Orosirian||c. 1835-1805 Ma||Includes the Mabel Downs Suite, Syenite Camp Suite and Kevins Dams Suite.||Granites and felsic to mafic volcanics including adakites, tonalites and granodiorites.|
31785|Sally Downs Supersuite|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|Kimberley.||||||
31785|Sally Downs Supersuite|70851|5|Briefly described|p4-p5, p7, p12, p18-p19|Paleoproterozoic|Paleoproterozoic|Lamboo Province. Geophysical response is discussed. See also p23-p24, p28-p30, p35.|c. 1850-1800 Ma||Includes the Mabel Downs Suite, Syenite Camp Suite and the Kevins Dam Suite.||Granites and mafic magmatic rocks.|
31785|Sally Downs Supersuite|71113|4|Described|p96,99,101,109-111|Orosirian|Orosirian|Geological province: Central Zone, Lamboo Province, Halls Creek Orogen. Felsic and mafic magmatism (geochemistry indicates mantle-derived material) associated with Halls Creek Orogeny and intruded into Central Zone at 1835-1805 Ma. Voluminous granites and mafic magmatism stitched the Western, Cwntral and Eastern zones of the Lamboo Province. Nd isotopic analysis suggest that it formed above a subduction zone with addition of mantle-derived materials (Sheppard et al., 2001). In fault contact with exposed granulite-facies Tickalara Metamorphics in the Central Zone.|1835-1805 Ma||Includes Kevin Dam, Mabel Downs and Syenite Camp suites.|||21-AUG-19
31785|Sally Downs Supersuite|71140|5|Briefly described|p96, 99, 101, 109-111|Orosirian|Orosirian|Central Zone, Lamboo Province, Halls Creek Orogen. Associated with the Halls Creek Orogeny and the suturing of Kimberley and North Australian Cratons.|1835-1805 Ma.||Mabel Downs, Syenite Camp, Kevins Dam Suites.|Is faulted against Tickalara Metamorphics.|Voluminous granites and mafic rocks.|
31785|Sally Downs Supersuite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|1832+\3 to 1808+\-3 Ma (isotopic, inferred)||Includes Mabel Downs Suite, Syenite Camp Suite, Kevins Dam Suite, Emull Gabbro, McIntosh Suite, Wild Dog Creek Gabbro, Mount Fairbairn Monzogranite.||Medium- to coarse-grained, porphyritic biotite monzogranite, syenogranite, and granodiorite, layered mafic-ultramafic intrusions, Biotite-bearing norite, olivine gabbronorite, gabbronorite, and minor gabbro|
31785|Sally Downs Supersuite|71281|5|Briefly described|p422, p432|||Extensively intrudes the Lamboo Province. Emplaced during later stages of the 1835-1810 Ma Halls Creek Orogeny. Possible source of zircons in Tunganary Formation; tectonic implications discussed.||||Intrudes Halls Creek Group and Tickalara Metamorphics.|Granite and gabbro.|
31785|Sally Downs Supersuite|71397|5|Briefly described|p3-6,42|Orosirian|Orosirian|Geological province: Central Zone, Lamboo Province, Halls Creek Orogen.  Emplaced during Halls Creek Orogeny; intrudes into the entire Lamboo Province at c. 1832-1808 Ma (Halls Creek Orogeny; Page et al., 2001).|c. 1832-1808 Ma||Includes Kevins Dam Suite, Mabel Downs Tonalite.|||
31785|Sally Downs Supersuite|71873|5|Briefly described|p426-427,434,442-445|Orosirian|Orosirian|Geological province: Lamboo Province. Emplacement occurred at 1832-1808 Ma during Halls Creek Orogen, which sutured the Kimberley Craton (Central and Western zones) to the North Australian Craton (Eastern Zone) (Tyler et al., 2012).|1832-1808 Ma||Includes Kevins Dam Suite.||Crustally-derived adakites and syn-collisional potassic granites.|
31785|Sally Downs Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Halls Creek Orogen.|Max age 1832+/-3 Ma, min 1808+/-3 Ma.||||Granite, gabbro, and layered mafic--ultramafic intrusions.|
31785|Sally Downs Supersuite|72490|6|Mentioned|p5|Orosirian|Orosirian|Outcrop along the suture between the Central and Western Zones.|ca. 1832-1808 Ma||||Mainly felsic rocks.|
31785|Sally Downs Supersuite|73089|6|Mentioned|p40|Orosirian|Orosirian|North-northeasterly trending. Two granitic rocks from the southern Halls Creek Orogen are considered part of this unit (c. 1817 and 1808 Ma).|c.1850-1808 Ma[?]|||||
81572|Sally Malay Complex|71873|5|Briefly described|p426-427|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province. Nomenclature introduced in this study to replace Sally Malay Intrusion.||Unit of Sally Malay Suite.|Includes Savannah, Savannah North and Subchamber-D intrusions.|||
78623|Sally Malay Suite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.|||Includes 5 unnamed units.||Layered mafic-ultramafic intrusions: gabbro, orthopyroxenite, leucogabbro, leucogabbronorite, anorthosite, olivine gabbro, olivine gabbronorite, gabbronorite, troctolite, olivine leucogabbro, peridotite, dunite, wehrlite, harzburgite.|04-AUG-15
78623|Sally Malay Suite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_geologyp08_lut.csv.|||||Ilmenite and titaniferous magnetite-bearing gabbro and orthopyroxenite, leucogabbro, leucogabbronorite and anorthosite; rhythmic cycles. Olivine gabbro, gabbronorite, troctolite, peridotite, dunite, wehrlite, harzburgite and olivine gabbro.|
78623|Sally Malay Suite|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Central Zone. See 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|1846-1844 Ma (Inferred)||||Magnetite-bearing gabbro, orthopyroxenite; leucogabbro, leucogabbronorite, anorthosite; olivine gabbro, olivine gabbronorite, gabbronorite, leucograbbro, troctolite; peridotite, dunite, wehrlite, harzburgite|
78623|Sally Malay Suite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv.|1844-1846 Ma||||Ilmenite and titaniferous magnetite bearing gabbro, orthopyroxenite, leucogabbro, leucogabbronorite, anorthosite, olivine gabbro, olivine leucogabbro and olivine gabbronorite, peridotite and dunite.|
78623|Sally Malay Suite|70812|5|Briefly described|p6, p8, p11, p20, p22, p27-p28, p43|Orosirian|Orosirian|Central Zone of the Halls Creek Orogen, Lamboo Province. Mineralisation is described. |c. 1845 Ma||||Mafic to ultramafic intrusives.|
78623|Sally Malay Suite|70851|5|Briefly described|p4-p5, p18, p35|Paleoproterozoic|Paleoproterozoic|Lamboo Province. Emplaced at 22km depth contemporaneous with the Koongie Park Formation. Referred to as the Sally Malay Ultramafics on p35.|c. 1850-1800 Ma||||Mafic magmatics.|27-MAR-23
78623|Sally Malay Suite|71113|5|Briefly described|p99-100|Orosirian|Orosirian|Geological province: Central Zone, Lamboo Province, Halls Creek Orogen. Part of a suite of large gabbroic and layered mafic-ultramafic bodies intruding into the Central Zone. |c. 1841+\-3 Ma|||||
78623|Sally Malay Suite|71140|6|Mentioned|p99-100|Orosirian|Orosirian|Central Zone, Lamboo Province, Halls Creek Orogen. Resulted from 1845-1840 Ma rifting of Tickalara Metamorphics.|1841 +/- 3 Ma.||||Large gabbroic and layered mafic-ultramafic bodies.|
78623|Sally Malay Suite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|1846-1844 Ma (inferred)||||Magnetite-bearing gabbro, orthopyroxenite; leucogabbro, leucogabbronorite, anorthosite; olivine gabbro, olivine gabbronorite, gabbronorite, leucograbbro, troctolite; peridotite, dunite, wehrlite, harzburgite|
78623|Sally Malay Suite|71873|5|Briefly described|p426-427,439,442|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province. Equivalent to the c. 1845 Ma Group V intrusions of Hoatson (2000) in the Central Zone. Includes over 14 mafic-ultramafic intrusions.|||Includes Wilson Creek and Dave Hill intrusions, and Sally Malay Complex.|||
78623|Sally Malay Suite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Central Zone, Halls Creek Orogen.|||||Layered mafic--ultramafic intrusions.|
80512|Salt Creek Gabbro|69743|6|Mentioned|p191|Mesoproterozoic|Mesoproterozoic|Is presented as Salt Creek Complex.||||||
80512|Salt Creek Gabbro|70802|5|Briefly described|250k_pre_mesozoic_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen. Events: Albany-Fraser Orogeny Stage II (1225-1140 Ma); Albany-Fraser Orogeny (1330-1140 Ma); Albany-Fraser Orogeny Stage I (1330-1260 Ma).|1300-1000 Ma (inferred)||||Gabbro or gabbronorite; locally intrusive into metasedimentary rocks|
80512|Salt Creek Gabbro|71270|4|Described|500k_interpgeop16_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: West Australian Craton. Events: Albany-Fraser Orogeny Stage II (1225 - 1140 Ma); Albany-Fraser Orogeny (1330 - 1140 Ma); Albany-Fraser Orogeny Stage I (1330 - 1260 Ma).|1300-1000 Ma (inferred)||||Gabbro or gabbronorite; locally intrusive into metasedimentary rocks|
80512|Salt Creek Gabbro|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Albany-Fraser Orogen.|||||Gabbro or gabbronorite; locally intrusive into metasedimentary rocks.|
30327|Salt River Group|22769|4|Described|p753,Fig2p754,757|||A palaeochannel system of sediments. Comprises: South Caroline Clay, Yenyening Formation and Quairading Sandstone. Possibly Oligocene to Pliocene age. In Yilgarn Craton area.||||||17-JAN-06
30327|Salt River Group|65194|5|Briefly described|p124 Fig.4.30|||Includes Yenyening Formation and South Caroline Clay.||||||
36640|Salt Well Member|50302|5|Briefly described|Map Legend|Archean|Archean|Of the Paradise Plains Formation. Geological Province: Pilbara Craton.||||||19-JUN-14
36640|Salt Well Member|63420|5|Briefly described|Map legend|Archean|Archean|Of Bookingarra Formation (Croydon Group, Pilbara Supergroup). Geological Province: Pilbara Craton. Mafic and volcanic and intrusive rocks; includes debris-flow deposits; metamorphosed.||||||07-NOV-08
36640|Salt Well Member|63441|5|Briefly described|p5 Tb.1, p29|Archean|Archean|Of Bookingarra Formation (Croydon Gp, Pilbara Supergp).Redefined from Paradise Plains Fm. Geological province: Mallina Basin, Pilbara Craton. Mafic volcanic rocks including volcaniclastic deposits and local vesicular and pillowed subaqueous flow units.||||||07-FEB-11
36640|Salt Well Member|64632|6|Mentioned|p203|||Basalt on northern margin of the East Pilbara terrrane. Compared to Loudens and Negri Volcanic Members, and Coonieena Basalt Member.|||||Basalt interbedded with clastic sedimentary rocks.|
36640|Salt Well Member|67201|5|Briefly described|p21 Fig.12, p61|||In northwestern Pilbara Craton, West Pilbara Superterrane and East Pilbara Terrane, De Grey Superbasin, Mallina Basin.||Bookingarra Formation||||
36640|Salt Well Member|68283|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Mallina and Lalla Rookh Basins.||Of the Bookingarra Formation.|||Mafic volcanic and intrusive rocks; includes debris-flow deposits; metamorphosed.|07-JAN-15
36640|Salt Well Member|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Croydon Group|||Metadolerite; mainly high-level intrusions, but may include flows; metamorphosed. Basaltic volcaniclastic deposits and vesicular and pillowed subaqueous basalt flows. Pyroxene spinifex textured basalt; locally pillowed.|
36640|Salt Well Member|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton. Of Mallina and Lalla Rookh basins, De Grey Superbasin. Events: North Pilbara Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|2964-2943 Ma (inferred)|Unit of Lalla Rookh Sandstone.|||Dolerite; mainly high-level intrusions, but may include flows; metamorphosed; pyroxene spinifex-textured basalt and basaltic volcaniclastic deposits and vesicular and pillowed subaqueous basalt flows; weakly metamorphosed.|
36640|Salt Well Member|70775|5|Briefly described|p11, p50, p59, p64|Mesoarchean|Mesoarchean|Originally included in the 'Paradise Plains Formation' before that unit was made obsolete by Van Kranendonk et al., 2006 (when they correlated it with the Lalla Rookh Sandstone).|c. 2950 Ma|Lalla Rookh Sandstone|||Mafic volcaniclastic deposits, pillowed and vesicular basalt flows and dolerite intrusions.|
36640|Salt Well Member|72668|6|Mentioned|p15|||Northern margin of the East Pilbara.||||||
35575|Salvation Group|24017|4|Described|p27|Mesoproterozoic|Mesoproterozoic|Replaces part of the Sunbeam Group.||||||12-FEB-07
35575|Salvation Group|24161|6|Mentioned|p23|Mesoproterozoic|Mesoproterozoic|||||||
35575|Salvation Group|24183|5|Briefly described|p2 Fig.1, p20|Mesoproterozoic|Mesoproterozoic|Geological Province: Blake Sub-basin. Overlies the Collier Group.||||||17-NOV-08
35575|Salvation Group|24535|5|Briefly described|p1, 2-5, 10, 12-15|Stenian|Mesoproterozoic|Siliciclastic sedimentary rocks. Intruded by Glenayle Dolerite, giving minimum age of deposition: 1066+/-14 Ma. Palaeolatitude of 30 degrees N.|||Includes Jilyili, Brassey Range and Coonabildie Formations.|||07-OCT-14
35575|Salvation Group|50195|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Bangemall Supergroup. Includes Glass Spring and Coonabildie Formations. Intruded by Glenayle Dolerite. Geological Province: Salvation Basin.||||||22-MAY-08
35575|Salvation Group|50222|5|Briefly described|p319 Fig. 2, p334 Tb. 2|Mesoproterozoic|Mesoproterozoic|Age: <1.46-1.22Ga and 1.20-1.10Ga.  Intruded by mafic sills and dykes of Glenayle Dolerite.||||||
35575|Salvation Group|50225|5|Briefly described|p386 Fig. 1|||Mentioned in terms of equivalents.||||||07-FEB-11
35575|Salvation Group|50319|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes the Brassey Range and Coonabildie Formations.||||||09-JUN-04
35575|Salvation Group|62453|6|Mentioned|p52, 4|||Minimum age:1080Ma.||||||
35575|Salvation Group|63866|5|Briefly described|p163, p168|||Bangemall Basin. Detrital zircons suggest an age younger than 1200 Ma, thus it may be a time equivalent of the Collier Group.||Bangemall Supergroup|Includes the Coonabildie Formation and the Brassey Range Formation.|||
35575|Salvation Group|64580|6|Mentioned|map legend|||||||||
35575|Salvation Group|64655|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes Brassey Range Formation and Coonabildie Formation.||||||
35575|Salvation Group|64724|5|Briefly described|p48, p49 Fig. 7|Stenian|Stenian|Collier Basin. Deposited during the Warakurna Event (1090-1050 Ma). Lies unconformably over the folded lower units of the Collier Basin.||||||
35575|Salvation Group|64728|6|Mentioned|p94 Fig.1. |||||||||
35575|Salvation Group|64772|4|Described|p13, Plate 1, 18-21,25-26,40,43, more|Mesoproterozoic|Mesoproterozoic|Includes Coonabildie, Glass Spring, Brassey Range and Jilyili Formations. Age: <1300 detrital ziron in underlying Collier Group, >1070 Ma, dolerite intrusions.Confusing age statements p13.  Geol.prov: NW Officer Basin in north and Collier/Earaheedy Basins in south. Also written as "Salvation Group".||Bangemall Supergroup||Overlies (may be conformable on) Collier Group;  intruded by Glenayle Dolerite||25-NOV-13
35575|Salvation Group|65506|5|Briefly described|p986, p987 Fig.1B||< 1200 Ma.|Present in the east of Capricorn Orogen. Sedimentary rocks comprise coastal deposits of cross bedded sandstone and siltstone with interbedded stromatolitic dolomite and evaporites. U-Pb dating detrital zircons. Part of Bangemall Supergroup.||||||
35575|Salvation Group|66427|5|Briefly described|p41 Tb.1, p42, p43 Fig 2., p45  |||Deposition 1.20->1.07 Ga. Mildly deformed by Edmundian Orogeny.||Of the Bangemall Supergroup.||Intruded by Glenayle Dolerite.||
35575|Salvation Group|67195|6|Mentioned|p6|||||||||
35575|Salvation Group|68055|6|Mentioned|p76-77|||Bangemall Superbasin.||Bangemall Supergroup.||||
35575|Salvation Group|69003|5|Briefly described|vi, p4, p13 Fig.17, p15, p41, p53, p72|Mesoproterozoic|Mesoproterozoic|Salvation Basin, Capricorn Orogen. Rims the NW Officer Basin.||||Overlies the Scorpion Group (and possibly lower Collier Group). Is intruded by Glenayle Dolerite.||
35575|Salvation Group|69091|5|Briefly described|p180|Mesoproterozoic|Mesoproterozoic|Regional outcrop trends in eastern Capricorn Orogen suggest Salvation Group overlies, and may interfinger with, upper Collier Group, rather than being equivalent, as suggested by Grey et al. (2005), and thus probably forms part of Collier Basin. Min age: dolerites intrude at 1066 +/- 14 Ma (Wingate, 2003). Max depositional detrital zircon age, ~1330 Ma, but with large error (Nelson, 2002).|max: ~1330 Ma, min: 1066 +/- 14 Ma; see comments||||Sandstone.|
35575|Salvation Group|69185|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Bangemall Supergroup.|Includes Glass Spring Formation, Jilyili Formation.|||
35575|Salvation Group|69596|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||||||
35575|Salvation Group|70768|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Salvation Basin.|1229-1080 Ma.|Bangemall Supergroup.|Glass Spring Formation.|||25-NOV-16
35575|Salvation Group|70795|5|Briefly described|2_5m_interpgeop15_lut.csv|Mesoproterozoic|Mesoproterozoic||1229-1080 Ma||||Sandstone and siltstone; lesser conglomerate.|
35575|Salvation Group|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Salvation Basin. Capricorn Orogen.||||||
35575|Salvation Group|71269|5|Briefly described|1m_geologyp12_lut.csv||||||Includes Coonabildie Formation.|||
35575|Salvation Group|72034|6|Mentioned|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Jilyili Formation, Glass Spring Formation, Brassey Range Formation, Coonabildie Formation.|||
35575|Salvation Group|72705|6|Mentioned|p3|||Capricorn Orogen.||||||
79800|Samphire Marsh Member|73344|2|Defined|p. 1, 3-6, 8-11, 13, 17-18, 20-21, 23...|earliest Dapingian|Tremadocian|Canning Basin, central-western. Proposed new upper subdivision of the Nambeet Formation [article includes definition card]. Type section is from the Olympic 1 well between 1170.00 and 1383.57 m = 213.57 m thickness. Varies between ~50 m to ~640 m. Contains two distinct mudstone-dominated sequences that grade upwards into carbonate-dominated units. Basal boundary marked as the contact with underlying sandstone (probably disconformable); top boundary is transitional, marked as where the core becomes ~100% carbonate (HyLogger); although this definition was said to be flawed. Named for the Samphire Marsh 1 well where the original type section for the formation is designated. Known only from the subsurface. Described using seven carbonate facies associations from eight key facies [article includes detailed lithologic description]. Reflects deposition on an epeiric platform or a very low-angle carbonate/epeiric ramp setting; transgressive to falling stage deposits. Records abrupt shutoff of siliciclastic input. Good hydrocarbon source potential, particularly the lower mudstone portion. Part of supersequence A. Covers part of the P. proteus and J. gananda conodont biozone and the entirity of the P. opeki - S. bilobatus and O. communis biozones. Other macrofossils such as trilobites, graptolites, brachiopods, bivalves and nautiloids sensu lato were identified as well as marine microfossils and bioturbation. Ages are bracketing bentonite U-Pb CA-ID-TIMS ages from Normore et al., (2018). Porosity and permeability are low in Olympic 1; poor reservoir potential. Contains two organic-rich zones in mudstone-dominated intervals. Minor quantities of gas have been recorded, and rare residual hydrocarbons in some wells. More locations: p. 29, 31-36, 39-41, 43, 47, 52-53, 55-56, 59-60, 62-64, Pl.1-2.|479.37 +/- 0.16 Ma to 470.18 +/- 0.13 Ma|Nambeet Formation||Underlain by Fly Flat Member. Overlain by Willara Formation and unconformably by Grant Group. Equivalent to Wilson Cliffs Sandstone, Gap Creek Formation, Emanuel Formation, and Kudata Dolomite.|Dominated by mudstone and carbonate. Limestone bed textures range from grainstone to lime mudstone and nodule textures vary from wackestone to lime mudstone. Mudstones in both interbedded and nodular sections are calcareous.|
79800|Samphire Marsh Member|73345|4|Described|p226-227, p229-231|Floian|Tremadocian|Canning Basin. Fly Flat/Samphire Marsh members pair demonstrates (limited) potential for a CO2 storage reservoir/seal pair. Type section from Olympic 1 well on the Broome Platform. Identified in Barnicarndy 1 based on conodonts; here it is a highly fossiliferous, organically lean calcareous mudstone unit with minor siltstone to very-fine-grained sandstone beds in the upper section and multiple bentonite beds throughout. Unit is more than four times thicker in Barnicarndy 1 (925 m) than the type section in Olympic 1.||Nambeet Formation||Conformably underlain by Fly Flat Member. Conformably overlain by Barnicarndy Formation.|Interbedded and nodular carbonate and mudstone sequences; limestone textures range from grainstone to wackestone, with mudstones generally calcareous and containing carbonate nodules.|
80961|Samuel Formation and Bejah Claystone|72034|5|Briefly described|500k_interpgeop16_lut|Albian|Aptian|Gunbarrel Basin. Informal combination of units for map scale.  Age from biostratigraphy.|||||Siltstone, sandstone and claystone; carbonaceous, locally glauconitic; radiolarian siltstone in Bejah Claystone.|
22810|San Sou Monzogranite|22496|5|Briefly described|p9|Statherian|Statherian|1788 +/- 6 Ma||||||
22810|San Sou Monzogranite|22716|6|Mentioned|p236|Statherian|Statherian|Age: 1790Ma.||||||09-DEC-08
22810|San Sou Monzogranite|22754|5|Briefly described|p7|Paleoproterozoic|Paleoproterozoic|Of San Sou Suite.  Age: c. 1790 Ma.||||||09-DEC-08
22810|San Sou Monzogranite|23599|5|Briefly described|p15|Paleoproterozoic|Paleoproterozoic|Age: c.1790 Ma. Geological Province: Lamboo Complex||||||07-NOV-08
22810|San Sou Monzogranite|44693|5|Briefly described|Map Legend||Proterozoic|||||||
22810|San Sou Monzogranite|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the San Sou Suite. Used interchangeably with San Sou Granite.||||||07-NOV-08
22810|San Sou Monzogranite|62580|6|Mentioned|p76|||In the Halls Creek Orogen.||||||07-FEB-11
22810|San Sou Monzogranite|63866|5|Briefly described|p129-p130, p138|||Eastern Zone, Halls Creek Orogen.|c. 1788 Ma|||||
22810|San Sou Monzogranite|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Fine to coarse grained biotite syenogranite and monzogranite.||||||09-DEC-08
22810|San Sou Monzogranite|65413|6|Mentioned|p107.|Paleoproterozoic|Paleoproterozoic|Southern Halls Creek Orogen.|1790 ma.|||||
22810|San Sou Monzogranite|66845|4|Described|p537 Fig.3, p539 Tb.1|||See San Sou Granite.|1788+/-6 Ma SHRIMP U-Pb|San Sou suite|||two-mica monzogranite|
22810|San Sou Monzogranite|68078|6|Mentioned|p5, p24|Paleoproterozoic|Paleoproterozoic||1788 +/- 6 Ma|||||
22810|San Sou Monzogranite|68656|5|Briefly described|GEOL_LUT_CSV/500k_geologyp08_lut|Paleoproterozoic|Paleoproterozoic|Described with Eastman Granite.|||||Fine- to coarse-grained biotite syenogranite and monzogranite.|
22810|San Sou Monzogranite|69003|6|Mentioned|p21|Paleoproterozoic|Paleoproterozoic|Intrudes the Kimberley Basin coevally with the c.1799-1795 Ma Hart Dolerite.||||||
22810|San Sou Monzogranite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic||||||Medium- to fine-grained biotite monzogranite; scattered fine-grained mafic inclusions.|04-AUG-15
22810|San Sou Monzogranite|69587|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Fine to course grained biotite syenogranite and monzogranite|
22810|San Sou Monzogranite|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|1788-1788 Ma (Isotopic)||||Medium- to fine-grained biotite monzogranite; scattered fine-grained mafic inclusions|
22810|San Sou Monzogranite|70154|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv.|1788 Ma||||Medium-fine grained biotite monzogranite; scattered fine grained mafic inclusions.|
22810|San Sou Monzogranite|70812|6|Mentioned|p29|||||||||
22810|San Sou Monzogranite|70826|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|Intruded during intracratonic reactivation of the Capricorn Orogen.||||||
22810|San Sou Monzogranite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|1788+\-6 Ma (isotopic)|Unit of San Sou Suite.|||Medium- to fine-grained biotite monzogranite; scattered fine-grained mafic inclusions|
22810|San Sou Monzogranite|71397|6|Mentioned|p5|Statherian|Statherian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen.||||||
22810|San Sou Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Halls Creek Orogen.|1788+/-6 Ma||||Medium- to fine-grained biotite monzogranite; scattered fine-grained mafic inclusions.|
22810|San Sou Monzogranite|72437|6|Mentioned|p11, p110|Palaeoproterozoic|Palaeoproterozoic|||San Sou suite||||
22810|San Sou Monzogranite|73089|6|Mentioned|p40-41|Statherian|Statherian|Halls Creek Orogen, southern.|1788 +/- 6 Ma|||||
74206|Sandbar Sandstone|61542|5|Briefly described|p277 Fig. 2, p285|Visean|Visean|Newly added to the Weaber Group -  forms part of revision by authors. Overlain by Sunbird Fm.which may(?) truncate it, or it pinches out. Geological Province: onshore Bonapart Basin/offshore Petrel-Sub-basin. tyep section in offshore Sandbar-1.||||Overlain by Sunbrid Formation. Overlies Tanmurra Fm.||26-NOV-18
74206|Sandbar Sandstone|69452|5|Briefly described|p36:12, 14-15, 17|Carboniferous|Carboniferous|||Weaber Group.||Unconformably overlies Tanmurra Formation. Is overlain unconformably by Sunbird Formation.||12-JUL-16
74206|Sandbar Sandstone|69653|6|Mentioned|p10|Carboniferous|Carboniferous|Petrel Sub-basin.||Weaber Group.||Overlies Tanmurra Formation. Is overlain by Sunbird Formation.||
74206|Sandbar Sandstone|69673|6|Mentioned|p168 fi, p 138, p171|Carboniferous|Carboniferous|||Weaber Group||||
74206|Sandbar Sandstone|70061|5|Briefly described|Petrel Sub-basin Fig.3|Visean|Visean|See also Regional geology: Fig.8.||Weaber Group.||Overlies Tanmurra Formation. Is overlain by Sunbird Formation.||12-JUL-16
74206|Sandbar Sandstone|73117|6|Mentioned|p15|Visean|Visean|Bonaparte Basin, southern.||Weaber Group||Underlain by Tanmurra Formation. Equivalent to Sunbird Formation.||
74623|Sandfire Calcilutite|64449|2|Defined|p75, p76, p79 Tb. 5, p91-95|Holocene|Holocene|Includes; Lagrange Calcilutite Member, Crab Creek Calcilutite Member and Djugun Member. Overlies: Port Smith Sand. Age: 1390+/-170 yrs BP and 7450+/-190 yrs BP (see p95) White/cream/grey bioturbated, laminated, locally indurated calcilutute.||||||07-FEB-11
74623|Sandfire Calcilutite|73213|5|Briefly described|958 Fig.3(a), 965 Fig.13||||||Djugun Member; Crab Creek, Lagrange, Calcilutite Members.|Overlies Mowanjum Sand.|High-mid tidal flat mud.|
23956|Sandpiper Sandstone|13194|4|Described|p385 Tb. 4-16, p396 fig 4-60|Berriasian|Tithonian|Type section Petrel 1 well (1329-1571m).||Flamingo Group||Overlies Frigate Shale (conformably).|Fine to coarse grained glauconitic sandstone.|
23956|Sandpiper Sandstone|13234|6|Mentioned|p260, p263 Tb.4.|||Reservoir quality sandstones.||Unit in Flamingo Group.||||
23956|Sandpiper Sandstone|22663|6|Mentioned|NT97 -1-4 Fig.4|||||||||
23956|Sandpiper Sandstone|23376|4|Described|p244||Berriasian|In the Bonaparte Basin.||||||29-NOV-06
23956|Sandpiper Sandstone|24047|5|Briefly described|p13|Jurassic|Jurassic|Geological Province: Money Shoal Basin.||||||
23956|Sandpiper Sandstone|24427|5|Briefly described|p49 Fig.2|Berriasian|Tithonian|Geological Province: Bonaparte Basin.||||||
23956|Sandpiper Sandstone|24569|5|Briefly described|p248 Fig. 3|Berriasian|Berriasian|Of the Flamingo Group.  Age:~140Ma.  Geological Province: Petrel Sub-basin.||||||02-MAR-05
23956|Sandpiper Sandstone|41459|6|Mentioned|Fig.2|||||||||
23956|Sandpiper Sandstone|41532|3|Fully described|p305|||||||||
23956|Sandpiper Sandstone|41731|6|Mentioned|Fig.3|||||||||
23956|Sandpiper Sandstone|42442|2|Defined|p26|Berriasian|Tithonian|Variation of Sandpiper Sandstone, WA. Age latest Jurassic to earliest Cretaceous||||||
23956|Sandpiper Sandstone|43661|6|Mentioned|Fig.3|||||||||
23956|Sandpiper Sandstone|43699|6|Mentioned|Fig.6,p10||Early Cretaceous|||||||
23956|Sandpiper Sandstone|49637|5|Briefly described|Fig. 3|Neocomian|Neocomian|Of the Flamingo Group. Geological Province: Petrel Sub-basin.||||||07-FEB-11
23956|Sandpiper Sandstone|60386|6|Mentioned|p302|Early Cretaceous|Late Jurassic|Bonaparte Basin. ||||||
23956|Sandpiper Sandstone|62837|5|Briefly described|Stratigraphic columns|Late Jurassic|Late Jurassic|Of the Flamingo Group. Age: ~142-~136Ma. Geological Province:  Petrel Sub-basin.||||||01-MAR-10
23956|Sandpiper Sandstone|64689|5|Briefly described|p7 Fig.6 |Early Cretaceous|Late Jurassic|Tithonian to Berriasian.||||||
23956|Sandpiper Sandstone|64696|6|Mentioned|p127 Fig.2 |Berriasian|Tithonian|||||||
23956|Sandpiper Sandstone|69452|5|Briefly described|p36:8, 15, 21-22|Early Cretaceous|Late Jurassic|Petrel Sub-basin, Bonaparte Basin. 30-270m thick.||Flamingo Group.||Overlies Frigate Shale.|Fluvial to deltaic sandstone-dominated unit.|12-JUL-16
23956|Sandpiper Sandstone|69653|5|Briefly described|p1, 6, 8, 10, p13 Fig.2.4, p15, 17-18|Cretaceous|Cretaceous|Petrel Sub-basin. Suitable for CO2 storage; sealed by Bathurst Island Group. Shallowing marine environment; fluvial to shoreface sediments. Schematic (gamma ray) well sections. Composite well diagram. Photomicrographs. See also p26-27, 30, 36-39, 41-43, 47-48, 50-53, 59-60, 63, 70, 73-76.||Flamingo Group.||Overlies Frigate Shale. Is overlain by Echuca Shoals Formation.|Mudstone; fine-grained sandstone interbedded with shale; massive fine-grained sandstone; fine- to coarse-grained sandstone. Facies described in detail.|
23956|Sandpiper Sandstone|69673|6|Mentioned|p173|||||Flamingo Group||||
23956|Sandpiper Sandstone|69689|6|Mentioned|p16|Cretaceous|Cretaceous|Bonaparte Basin.||||||
23956|Sandpiper Sandstone|70061|5|Briefly described|Petrel Sub-basin; Fig.2|Valanginian|Berriasian|See also Regional geology: Figs.6-7, p12, p19. Sahul: Fig.2, p2. Vulcan: Fig.2. Marine shelf and possibly slope and basin-floor fan complexes. A secondary reservoir in the N Bonaparte Basin. Hosts gas in anticlinal, fault block and stratigraphic traps (Saratoga 1).||Flamingo Group.||Overlies Upper Frigate Shale. Is overlain by Echuca Shoals Formation.|Quartzose clastics.|12-JUL-16
42367|Sandy Blight Quartzite|61387|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Interlayered and strongly foliated quartzite and quartz-muscovite schists. Of the Kintore Domain, Warumpi Province.  In the Arunta region.||||||07-NOV-08
42367|Sandy Blight Quartzite|61519|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Interlayered and strongly foliated quartzite and quartz muscovite schist. Geological Province: Warumpi Province||||||07-NOV-08
42367|Sandy Blight Quartzite|65358|6|Mentioned|p24|||1100 +/- 5 Ma age for muscovite from quartz vein (Wygralak and Mernagh, 2004).||||||
42367|Sandy Blight Quartzite|68994|5|Briefly described|p4|||Kintore Domain in Warumpi Province.|||||Quartzite and phyllite.|
42367|Sandy Blight Quartzite|69428|5|Briefly described|p13:2-3, 12, 15|Paleoproterozoic|Paleoproterozoic|Close et al. (in prep). Kintore Domain, Warumpi Province. Forms a series of isolated hills and ridges extending for 45km W from near Sandy Blight Junction. Greenschist facies metamorphism. Timing of deposition is uncertain. SHRIMP U-Pb detrital zircon maximum deposition age.|1680 +/- 3 Ma (Worden et al., 2006).||||Crystalline metasedimentary quartzite containing a variably defined muscovite foliation, with less abundant quartz-muscovite phyllite that contains a bedding-parallel cleavage and 5-20cm-thick quartzite interbeds.|12-JUL-16
42367|Sandy Blight Quartzite|69933|5|Briefly described|v, p1, p18-21, p37|Statherian|Statherian|Petrography, zircon characteristics, SHRIMP analyses and results are provided.|1681 +/- 8 Ma (Max dep age, SHRIMP U-Pb)||||Crystalline metasedimentary quartzite containing a variably defined muscovite foliation.|21-APR-23
42367|Sandy Blight Quartzite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||pelite, greenstone, schist, quartzite|
42367|Sandy Blight Quartzite|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1681+/-8 Ma (MDA: U-Pb zircon SHRIMP)||||Quartzite.|
42367|Sandy Blight Quartzite|72360|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological province: Warumpi Province. Of Kintore Domain.|||||Foliated quartzite and quartz-muscovite schist.|09-SEP-19
22815|Sandy Dam Monzogranite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.||||||07-NOV-08
22815|Sandy Dam Monzogranite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1850Ma. Geological province: Kimberley Province (East).||||||07-FEB-11
22815|Sandy Dam Monzogranite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
22815|Sandy Dam Monzogranite|43854|5|Briefly described|Map Legend||Proterozoic|||||||
22815|Sandy Dam Monzogranite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
22815|Sandy Dam Monzogranite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite.||||||07-NOV-08
22815|Sandy Dam Monzogranite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Paperbark Supersuite|Includes unnamed sub-unit.||foliated, medium- to coarse-grained biotite metamonzogranite; minor fine-to medium-grained biotite metagranodiorite and metatonalite|
22815|Sandy Dam Monzogranite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Paperbark Supersuite|||Foliated, medium to coarse grained biotite metamonzogranite;  fine to medium grained, equigranular biotite metagranodiorite and metatonalite.|
22815|Sandy Dam Monzogranite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone.|1864-1852 Ma (Inferred)|Unit of Paperbark Supersuite.|||Foliated, medium- to coarse-grained biotite metamonzogranite; minor fine-to medium-grained biotite metagranodiorite and metatonalite|
22815|Sandy Dam Monzogranite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1852-1864 Ma|Paperbark Supersuite|||Foliated medium to coarse grained biotite metamonzogranite; fine to medium grained biotite metagranodiorite and metatonalite.|
22815|Sandy Dam Monzogranite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (183 -1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1864-1852 Ma (inferred)|Unit of Paperbark Supersuite.|||Foliated, medium- to coarse-grained biotite metamonzogranite; minor fine-to medium-grained biotite metagranodiorite and metatonalite with small clots of biotite; locally hornblende bearing|
22815|Sandy Dam Monzogranite|72437|5|Briefly described|p82, p84-85|||Lamboo Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Foliated porphyritic biotite monzogranite.|
35666|Santa Ana Trondhjemite|23137|5|Briefly described|p250 Fig.3|||||||||
35666|Santa Ana Trondhjemite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||3010 - 2600 Ma (inferred).||||Medium-grained tonalite-trondhjemite; plagioclase-biotite-muscovite-quartz; massive to strongly foliated; metamorphosed.|
35666|Santa Ana Trondhjemite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|3010-2600 Ma (inferred)||||Medium-grained tonalite-trondhjemite; plagioclase-biotite-muscovite-quartz; massive to strongly foliated; metamorphosed|
35606|Santa Claus Member|23582|5|Briefly described|Map Legend|Archean|Archean|Of Mount Belches Formation. Iron formation unit comprising wacke, mudstone and ferruginous mudstone.||||||07-NOV-08
35606|Santa Claus Member|23584|2|Defined|p37 Appendix 2|Archean|Archean|Of Mount Belches Formation. Geological Province: Yilgarn Craton. Max. thickness: 150 m.||||||07-NOV-08
35606|Santa Claus Member|60555|5|Briefly described|p11|||Banded-iron formation, forms chevron fold patterns and complex fold-interface structures. Contains finley banded magnetite-quartz rocks, magnetite-rich graded wacke-mudstone units, and amphibolitic rocks (Painter and Groenewald, 2001).||||||30-NOV-09
35606|Santa Claus Member|65264|5|Briefly described|p21|||Of Mount Belches Formation. A distinctive sequence of turbiditic iron-formation.||||||07-FEB-11
35606|Santa Claus Member|66937|5|Briefly described|pp160-162.|Archean|Archean|Chert beds are diagenetic in origin and their top surfaces are siliceous hardgrounds. Siderite was the probable precursor to metamorphic magnetite.||Unit in Belches Supersequence.|||Three packages of sandstone-mudrock each ending in a 1-2 m-thick bed of chert-magnetite.|
35606|Santa Claus Member|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton||Mount Belches Formation|||Wacke, mudstone, and ferruginous mudstone laterally grading into cherty iron-formation; common Bouma sequences with magnetite concentrated in the pelitic portion; metamorphosed.|07-AUG-15
35606|Santa Claus Member|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|||Mount Belches Formation|||Wacke, mudstone, and ferruginous mudstone laterally grading into cherty iron-formation; common Bouma sequences with magnetite concentrated in the pelitic portion; metamorphosed.|
35606|Santa Claus Member|70802|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton.||Unit of Mount Belches Formation.|||Wacke, mudstone, and ferruginous mudstone laterally grading into cherty iron-formation; common Bouma sequences with magnetite concentrated in the pelitic portion; metamorphosed|
35606|Santa Claus Member|71270|4|Described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton.||Unit of Mount Belches Formation.|||Wacke, mudstone, and ferruginous mudstone laterally grading into cherty iron-formation; common Bouma sequences with magnetite concentrated in the pelitic portion; metamorphosed|
78348|Satellite Igneous Complex|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2720 - 2660 Ma (inferred).||||Dolerite, gabbro; metamorphosed. Strongly foliated mafic amphibolite. Serpentinite, pyroxenite - commonly altered to tremolite. Peridotite including adcumulate dunite and minor pyroxenite; metamorphosed.|19-MAY-21
78348|Satellite Igneous Complex|71212|5|Briefly described|intro p2, intro p3|||Yilgarn Craton. Equivalent to the informal Cemetery layered mafic-ultramafic complex. ||||Overlies (and is interbedded with) the Hickies Bore Basalt. Overlain by the Songvang Formation or the Fourteen Mile Well Formation.||
78348|Satellite Igneous Complex|73151|6|Mentioned|p3|||Yilgarn Craton. Kalgoorlie Terrane, Agnew Greenstone Belt. Shown as Satellite IC.|||||Dolerite.|
73588|Satirist Monzogranite|63441|5|Briefly described|p11 Tb. 2|Archean|Archean|Of Sisters Supersuite. Supersedes Satirist Granite. Age: 2938+/-4Ma and 2931+/-5Ma. Geological province: Pilbara Craton/Mallina Basin.||||||07-FEB-11
73588|Satirist Monzogranite|64580|4|Described|map legend||Mesoarchean|Of Sisters Supersuite. Biotite(-hornblende) granite; metamorphosed.||||||15-DEC-08
73588|Satirist Monzogranite|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological Province: West Pilbara Granite-Greenstone Terrane, Central Pilbara Tectonic Zone, and southwest Pilbara inlier, Pilbara Craton. [Also referred to as Satirist Granite on 500k_interpgeop_pilcrat02_lut.csv]. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 2940-2930 Ma|Unit of Sisters Supersuite.|||Pyroxene-bearing, foliated to massive, medium- to coarse-grained alkali granite; metamorphosed|
73588|Satirist Monzogranite|69590|4|Described|500k_geologyp08_lut.csv|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; North Pilbara Orogeny.||Unit of Sisters Supersuite.|||Biotite(-hornblende) granite; metamorphosed|
73588|Satirist Monzogranite|70775|5|Briefly described|p29 tbl 5, p41, p43, p62, p63|Mesoarchean|Mesoarchean|Mallina Basin. Also dated at c. 3040 by Rb-Sr (Leggo et al;., 1965)|c. 2938-2931 Ma (Smithies et al 1998b)|||||
73588|Satirist Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
73588|Satirist Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||Max age 2938+/-4 Ma, min 2931+/-5 Ma|Sisters Supersuite|||Leucocratic monzogranite and syenogranite; metamorphosed.|
81324|Satisfaction Supersuite|70020|6|Mentioned|p122, 132|||Restricted to the eastern side of the northern Kalgoorlie Terrane and shows a strong spatial relationship with contemporaneous and partly cogenetic felsic volcanic rocks.|||Shown as including Gemchapps monzogranite p122.|||07-AUG-19
81324|Satisfaction Supersuite|71148|6|Mentioned|p122|Neoarchean|Neoarchean|Eastern Goldfields Superterrane.|||||HFSE-enriched granites.|
26135|Saunders Creek Formation|22496|6|Mentioned|p7||Paleoproterozoic|Of the Halls Creek Group.  In the Halls Creek Province.||||||07-NOV-08
26135|Saunders Creek Formation|22526|4|Described|P680, Fig3 P682||Orosirian|||||||
26135|Saunders Creek Formation|22754|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|Of the Halls Creek Group.||||||07-NOV-08
26135|Saunders Creek Formation|23383|6|Mentioned|p12|||Of Halls Creek Group.||||||25-JAN-05
26135|Saunders Creek Formation|23599|4|Described|p9|Paleoproterozoic|Paleoproterozoic|Age: c.1880 Ma. Of Halls Creek Group. Overlain by Biscay Formation; underlain by Junda Microgranite. Max. thickness: 150 m.||||||07-NOV-08
26135|Saunders Creek Formation|23621|4|Described|p15|Orosirian|Orosirian|See also p12 table 1. Of Halls Creek Group. Overlying unit Biscay Formation. Underlying unit Sophie Downs Granophyre member. Halls Creek Orogen. Max. thickness:  200 m.||||||
26135|Saunders Creek Formation|23622|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Halls Creek Group.||||||07-NOV-08
26135|Saunders Creek Formation|24173|3|Fully described|p15, p14 Tb.2|Paleoproterozoic|Paleoproterozoic|Basal sandstone and conglomerate of Halls Creek Group. Conformably overlain by Biscay Fm; unconformably overlies Ding Dong Downs Volcs. Geol Prov: Halls Creek Orogen.  Age: 3585-2508Ma (detrital zircons of Archaean derivation). See also p10 Tb.1 and p33.||||||07-NOV-08
26135|Saunders Creek Formation|30097|6|Mentioned|Fig.54|||Also Table 23.||||||29-NOV-06
26135|Saunders Creek Formation|30892|5|Briefly described|p94|||Archaean ?||||||
26135|Saunders Creek Formation|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26135|Saunders Creek Formation|32660|5|Briefly described|Table 1|||||||||
26135|Saunders Creek Formation|32728|5|Briefly described|Table 3|||||||||
26135|Saunders Creek Formation|33443|6|Mentioned|p261|||||||||
26135|Saunders Creek Formation|36551|6|Mentioned|Table 15|||||||||
26135|Saunders Creek Formation|36885|4|Described|p166|||||||||
26135|Saunders Creek Formation|36902|6|Mentioned|p11|||||||||
26135|Saunders Creek Formation|37462|4|Described|Table 4.I|||||||||
26135|Saunders Creek Formation|38557|6|Mentioned|p286|||||||||
26135|Saunders Creek Formation|41125|6|Mentioned|p12|||See also Fig.4||||||
26135|Saunders Creek Formation|41635|4|Described|p19|||||||||
26135|Saunders Creek Formation|41976|6|Mentioned|p453|||||||||
26135|Saunders Creek Formation|41977|5|Briefly described|p471|||||||||
26135|Saunders Creek Formation|41980|6|Mentioned|Fig.5 P587|||||||||
26135|Saunders Creek Formation|41987|6|Mentioned|Fig.3 P73|||||||||
26135|Saunders Creek Formation|42326|5|Briefly described|p9|||||||||
26135|Saunders Creek Formation|43299|5|Briefly described|Map Legend||Paleoproterozoic|Of the Halls Creek Group.||||||07-NOV-08
26135|Saunders Creek Formation|43561|6|Mentioned|p1437|||||||||
26135|Saunders Creek Formation|44155|4|Described|p234-236|Paleoproterozoic|Paleoproterozoic|0 - 200m thick.||Halls Creek Group||Disconformably overlies Ding Dong Downs Volcanics. Is overlain by Biscay Formation.|Cross-bedded quartzite, arkosic quartzite, lithic arenite and quartz conglomerate; interbedded, buff-coloured phyllite is prominent near the top of the sequence.|
26135|Saunders Creek Formation|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Halls Creek Group. Metamorphosed quartz sandstone, feldspathic sandstone, and quartz pebble conglomerate. Age: c.1880Ma. In the Lamboo Complex (eastern zone).||||||07-NOV-08
26135|Saunders Creek Formation|44317|14|Not recorded|p.5|||||||||
26135|Saunders Creek Formation|44324|14|Not recorded|p.5|||Tb.1. Of Halls Creek Group.  Archaean or Proterozoic.||||||29-NOV-06
26135|Saunders Creek Formation|44325|14|Not recorded|map legend|||Archaean or Proterozoic.||||||
26135|Saunders Creek Formation|44397|14|Not recorded|p.8, Table 1|||Of the Hall Creek Group. Archaean or Proterozoic.||||||29-NOV-06
26135|Saunders Creek Formation|44398|14|Not recorded|map legend|||Archaean or Proterozoic.||||||
26135|Saunders Creek Formation|44693|5|Briefly described|Map Legend||Proterozoic|||||||
26135|Saunders Creek Formation|45047|2|Defined|p62|Paleoproterozoic|Paleoproterozoic|See pp13-15. Of the Halls Creek Group.||||||07-NOV-08
26135|Saunders Creek Formation|45048|6|Mentioned|p10|||See also p65, Fig.13. Of the Halls Creek Group.||||||29-NOV-06
26135|Saunders Creek Formation|50437|6|Mentioned|p5.1|||Overlies: Sophie Downs Granite (unconformably). Of the Halls Creek Group.||||||
26135|Saunders Creek Formation|60724|4|Described|p4, p7|||Of the Halls Creek Group. Unconformably overlies Ding Dong Downs Volcanics and Sophie Downs Granite; conformably overlain by Biscay Formation. Within the Lamboo Complex.||||||
26135|Saunders Creek Formation|61056|6|Mentioned|p785 Tb. 2|||||||||
26135|Saunders Creek Formation|61861|6|Mentioned|Fig.2.|||Halls Creek, eastern zone.||Unit in Halls Creek Group.||Is overlain by Biscay Formation.||
26135|Saunders Creek Formation|63866|4|Described|p130|||Characterised by fluvial to shallow marine deposits dominated by Palaeo- to Neoarchean zircon detritus.|<1910 Ma|Halls Creek Group||Conformably overlain by the Biscay Formation.|Quartz sandstones and conglomerate.|
26135|Saunders Creek Formation|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Of Halls Creek Group. Sandstone and pebble conglomerate; metamorphosed.||||||09-DEC-08
26135|Saunders Creek Formation|66846|6|Mentioned|p549 Fig.2|Orosirian|Orosirian|In the Eastern Zone of the Lamboo Complex.|||||Terriginous clastic rock.|
26135|Saunders Creek Formation|68078|6|Mentioned|p7 figure 4|Paleoproterozoic|Paleoproterozoic||~1885 Ma|||||
26135|Saunders Creek Formation|68656|5|Briefly described|GEOL_LUT_CSV/500k_geologyp08_lut|Paleoproterozoic|Paleoproterozoic|||Halls Creek Group|||Sandstone and pebble conglomerate; metamorphosed.|
26135|Saunders Creek Formation|69003|5|Briefly described|p19|Paleoproterozoic|Paleoproterozoic|E zone, Lamboo Province, Halls Creek Orogen.|c.1880 Ma.|Halls Creek Group.||||
26135|Saunders Creek Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Data from OZCHRON1. Age: 2508+/-5 Ma. Comment: 'This is a maximum depositional age for the Saunders Creek Fmn. The actual stratigraphic age is much younger (1910-1880 Ma).|1910-1880 Ma|Halls Creek Group|||Quartzose and feldspathic metasandstone, and quartz-pebble metaconglomerate.|04-AUG-15
26135|Saunders Creek Formation|69165|4|Described|100k_interpgeop_lut.csv|Neoarchean|Paleoarchean|See also 500k_geologyp08_lut.csv, GA_geochron.csv. |2508-3225 Ma|Halls Creek Group|||Quartzose and feldspathic metasandstone, quartz pebble metaconglomerate.|
26135|Saunders Creek Formation|69585|6|Mentioned|p4|Orosirian|Orosirian|Eastern Lamboo Province.||Halls Creek Group.||||
26135|Saunders Creek Formation|69587|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|||Unit of Halls Creek Group.|||Sandstone and pebble conglomerate; metamorphosed|
26135|Saunders Creek Formation|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|1907-1880 Ma (Inferred)|Unit of Halls Creek Group.|||Quartzose and feldspathic metasandstone, and quartz-pebble metaconglomerate|
26135|Saunders Creek Formation|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1880-1907 Ma||||Quartzose and feldspathic metasandstone, quartz pebble metaconglomerate.|
26135|Saunders Creek Formation|70812|4|Described|p5, p7, p19|Orosirian|Orosirian|Eastern Zone of the Halls Creek Orogen, Lamboo Province.||Halls Creek Group||Unconformably overlies the Ding Dong Downs Volcanics. Overlain by the Biscay Formation.|Siliciclastic sedimentary rocks.|
26135|Saunders Creek Formation|70851|4|Described|p3, p5|Paleoproterozoic|Paleoproterozoic|Eastern Zone, Lamboo Province.||Halls Creek Group||Overlain by the Biscay Formation.|Siliciclastic sedimentary rocks.|
26135|Saunders Creek Formation|71113|5|Briefly described|p96-97|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen. Depositional environment: fluvial to shallow marine. Derived from Archean sources (Page and Sun, 1994).||Unit of Halls Creek Group.||Lowermost unit of Halls Creek Group. Overlain by Biscay Formation.|Quartz sandstone and conglomerate.|
26135|Saunders Creek Formation|71140|6|Mentioned|p96-97|Orosirian|Orosirian|Eastern Zone, Lamboo Province, Halls Creek Orogen.||Halls Creek Group.||Is overlain conformably by Biscay Formation.|Fluvial to shallow-marine quartz sandstone and conglomerate.|
26135|Saunders Creek Formation|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv and geochron files.|1909-1881 Ma (inferred)|Unit of Halls Creek Group.||Overlain conformably by Biscay Formation.|Quartzose and feldspathic metasandstone, and quartz-pebble metaconglomerate|
26135|Saunders Creek Formation|71397|3|Fully described|p1,3-5,7-8,10-12,14,19,22,30, 32-35|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen. Deposited in a high-energy fluvial environment with stacked channels typical of braided river systems to possibly lacustrine settings. Crops out as thin veneers, up to 200 m thick, unconformable on basement structural domes. Eastern zone D1 Halls Creek Orogeny deformation resulted in strong shear zone contact with underlying basement rocks. REE Geochemical analysis trends normalized to post-Archean Australian shales (PAAS). See p19 for detailed major and trace-element geochemical analysis. Zircon U-Pb geochronological analysis of sample GA 875980289 (quartz sandstone) yielded a weighted mean 207Pb*/206Pb* date of 2512+\-8 Ma, interpreted as maximum depositional age of sandstone protolith. Sample 08TKHCO03 (quartzite)  yielded a weighted mean 207Pb*/206Pb* date of 2508+\-8 Ma, interpreted as maximum depositional age of sandstone protolith. However a more robust maximum age constraint of sediment distribution is provided the underlying 1912-1904 Ma Ding Dong Downs basement. Dominated by Neoarchean to Paleoarchean detrital grains, similar to that in Brim Rockhole Formation. Absence of c. 1910 Ma zircons is consistent with a partially or locally buried basement (Sophie Downs Suite) during development of the fluvial system. See also p42-43,45-46,48.|c. 1904-1881 Ma|Unit of Halls Creek Group.||Lowermost unit of Halls Creek Group. Conformably overlain by Brim Rockhole Formation. Underlain unconformably by Ding Dong Downs Volcanics. Intruded by Woodward Dolerite.|Trough-cross-bedded quartzofeldspathic metasandstone interbedded with metaconglomerate; fines up locally.|28-NOV-19
26135|Saunders Creek Formation|71873|5|Briefly described|p426-427|Orosirian|Orosirian|Geological province: Lamboo Province. Depositioanl environment: fluvial. Intruded by Woodward Dolerite during Halls Creek Orogeny c. 1832-1808 Ma.|ca. 1875-1860 Ma detrital zircons.|Unit of Halls Creek Group.||||
26135|Saunders Creek Formation|73089|5|Briefly described|p24-27, p36|Orosirian|Orosirian|Lamboo Province, Eastern Zone. Relatively coarse grained, and transitions into fining-upwards packages of thin-bedded to laminated, sediment-starved metasedimentary units that include chemical sediments. Range of detrital zircon age components between c. 3600 and 2500 Ma.  Paleocurrent indicators have been measured from this unit (northwest-southeast axis).|1912-1904 Ma|||Unconformably underlain by Sophie Downs Suite. Overlain by Brim Rockhole Formation.||
81577|Savannah North intrusion|71873|5|Briefly described|p427-428,430-441|Orosirian|Orosirian|Geological province: Lamboo Province. Detrital zircon magmatic ages include 1839+\-5, 1846+\-6 and 1842+\-5 Ma. Cut by dolerite and microgranite dykes that yield U-Pb ages of 1842+\-3 and 1829+\-3 Ma respectively.||Unit of Sally Malay Complex.||Cross-cut by Turkey Creek Gabbro.|almost entirely peridotite and olivine gabbros interlayered on 10¿100mscale.|03-SEP-19
79545|Savannah intrusion|69003|4|Described|p22|Paleoproterozoic|Paleoproterozoic|E Kimberley region, Halls Creek Orogen. Formerly the Sally Malay intrusion. Consists of an array of ovoid-shaped chambers interconnected by feeder zones and dykes. Hosts significant Ni-Cu-Co sulfide mineralisation in a 40m thick basal norite.|1844 +/- 3 Ma.|||Intrudes Tickalara Metamorphics.|Layered mafic-ultramafic intrusion.|01-SEP-16
79545|Savannah intrusion|71873|5|Briefly described|p427-428,430-441|Orosirian|Orosirian|Geological province: Lamboo Province. Originally blade-shaped, it is a curved dyke-like body with parallel steeply-dipping sides and internal vertically-orientated layering. Mineralised Savannah Intrusion yields detrital zircon magmatic ages of 1843+\-6, 1846+\-5 and 1844+\-5 Ma. Cut by dolerite and microgranite dykes that yield U-Pb ages of 1842+\-3 and 1829+\-3 Ma respectively.||Unit of Sally Malay Complex.||Cross-cut by Turkey Creek Gabbro.|Interlayered cumulate peridotite, troctolite and olivine gabbronorite, transitioning upward to a sequence dominated by cumulate norite.|
76744|Scamp Formation|68995|5|Briefly described|p7 Fig.3, p13, p21, p24, p27-28, p43,p46|||Metamorphism briefly discussed.||Mount Palgrave Group||(Probably) overlies the Eliza Formation. Overlain by Mount Waugh rhyolite.|Garnet bearing granoblastic metarhyolites.|
76744|Scamp Formation|68996|6|Mentioned|p7, p36, p50, 65|Mesoproterozoic|Mesoproterozoic|Misspelt as Scamp Group p52.||Mount Palgrave Group|Includes Scamp granite|||
76744|Scamp Formation|69009|5|Briefly described|Map Legend|Stenian|Stenian|Bentley Basin.|1077-1063 Ma|Of the Mount Palgrave Group.|||Comprises rhyolite; possibly lava flows and pyroclastic rocks, but may include subvolcanic intrusions; typically shows a fine- to coarse-grained granofelsic texture, indicating weak to moderate recrystallisation.|
76744|Scamp Formation|69091|5|Briefly described|p71 Fig.4.14, p144|||Talbot Sub-basin. Presented as Scamp Fm in figure.||Mount Palgrave Group||||
76744|Scamp Formation|69153|5|Briefly described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen||Mount Palgrave Group|||Rhyolite, as lavas, pyroclastic rocks and subvolcanic intrusions|
76744|Scamp Formation|69729|6|Mentioned|p82|||Bedrock of Talbot Sub-basin.||Mount Palgrave Group.||||
76744|Scamp Formation|70095|5|Briefly described|p17,19|||Geological province: Musgrave Province. Of Talbot Sub-basin, Bentley Basin. See p19 Table 2 for U-Pb zircon data.||Unit of Mount Palgrave Group.||Overlain by Mount Waugh rhyolite. Underlain by Eliza Formation.||
76744|Scamp Formation|70134|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Mount Palgrave Group.||Is overlain (?conformably) by Mount Waugh Formation.|Rhyolite; possibly lava flows and pyroclastic rocks but may include subvolcanic intrusions; typically fine- to coarse-grained granofelsic texture indicating weak to moderate recrystallisation. Four facies variations are mapped separately.|
76744|Scamp Formation|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Two facies are mapped separately.||Mount Palgrave Group.||Is overlain by Mount Waugh Formation. Is intruded by Warakurna Supersuite.|Rhyolite, possibly lava flows and pyroclastic rocks but may include subvolcanic intrusions; typically shows a fine- to coarse-grained granofelsic texture indicating weak to moderate recrystallisation.|
76744|Scamp Formation|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|SHRIMP ages derived from rhyolite samples (195678.1.pdf)|1047 Ma - 1077 Ma (Inferred) 1064 Ma  (SHRIMP)||||Rhyolite lavas and pyroclastic rocks that show either a fine to coarse grained granofelsic texture or a fine grained granoblastic texture. Very fine grained-microcrystalline, spherulitic, pumiceous feldspar-porphyritic rhyolite.|
76744|Scamp Formation|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Sample GSWA 195673 (felsic granofels) yielded an interpreted (lower intercept on concordia) magmatic crystallisation age of 1059+\-6 Ma. Sample GSWA 195678 (rhyolite) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) magmatic crystallisation age of 1064+\-5 Ma. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyl_lut.csv.|1077-1047 Ma (inferred)|Unit of Mount Palgrave Group.||Underlain by Eliza Formation. Overlain by Mount Waugh Formation.|Rhyolite; possibly lava flows and pyroclastic rocks; aphyric, pumiceous rhyolite, feldspary-porphyritic rhyolite, rhyolitic pyroclastic block breccia.|
76744|Scamp Formation|71211|6|Mentioned|p216, p234|||||Mount Palgrave Group||||
76744|Scamp Formation|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Sample GSWA 195673 (felsic granofels) yielded a lower intercept on concordia of 1059+\-6 Ma , interpreted as magmatic crystallisation age of igneous protolith. Sample GSWA 195678 (rhyolite) yielded a concordia age of 1064+\-5 Ma, interpreted as magmatic crystallisation age of the rhyolite. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv.|1077-1047 Ma (inferred)|Unit of Mount Palgrave Group.||Overlain by Mount Waugh Rhyolite. Underlain by Eliza Formation.|Aphyric, pumiceous rhyolite; typically flow folded; very fine-grained to microcrystalline, spherulitic, pumiceous, feldspar-porphyritic rhyolite; rhyolitic pyroclastic block breccia.|
76744|Scamp Formation|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1059+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Fine-grained, massive to flow-banded rhyolite.|
76744|Scamp Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Mount Palgrave Group|||Rhyolite; possibly lava flows and pyroclastic rocks, but may include subvolcanic intrusions; typically shows a fine- to coarse-grained granofelsic texture, indicating weak to moderate recrystallization.|
76744|Scamp Formation|72094|6|Mentioned|p13|Mesoproterozoic|Mesoproterozoic|||Of Mount Palgrave Group.||||
76744|Scamp Formation|72443|6|Mentioned|p738, p742||||1070 +/- 9 Ma (SHRIMP U-Pb)|Mount Palgrave Group||||
81329|Scott Rock monzogranite|70023|4|Described|p170,184-186|Stenian|Stenian|Geological province: Madura Province; Eastern Nornalup Zone, Albany-Fraser Orogen. Also referred to as just Scott Rock, or Scott Rock granite in fig2 p170. Crystallisation age of 1175+\-12 Ma for the monzogranite at Scott Rock is typical of the ages of Esperance Supersuite granites (1200-1140 Ma, Kirkland et al., 2014). Intruded into Ragged Basin/Mount Ragged Formation. Post-dates Ragged Basin deformation and 1175+\-12 Ma monzogranite age provides minimum age of structural emplacement of Ragged Basin thrust slices.|1175+/-12 SHRIMP U-Pb zircon age.|||||07-AUG-19
31033|Scotty Creek Formation|23144|5|Briefly described|p162-163|||||||||
31033|Scotty Creek Formation|23145|4|Described|p157|||||||||
31033|Scotty Creek Formation|23929|5|Briefly described|p104|||Geological Province: Yilgarn Craton.||||||
31033|Scotty Creek Formation|24196|6|Mentioned|p69|||Formation is Fm in text.||||||
31033|Scotty Creek Formation|43776|5|Briefly described|p323|||||||||
31033|Scotty Creek Formation|69583|5|Briefly described|p39, p89-90, p92|||Western limb of Lawlers Anticline, Agnew area. Typical "late basin" sediments. Geochronology by Kositcin et al. (2008) on p39 but attributed to Dunphy et al. (2003) on p89 (twice). Seismic interpretation.|c.2662 Ma (maximum depositional age).|||Correlated with Merougil Group.|A thin basal package of conglomerate and sandstone, and thick quartz-rich clastic sedimentary rocks.|
31033|Scotty Creek Formation|69586|5|Briefly described|p1, p11-13, p15|||Crops out between the Waroonga Shear Zone and the Emu Fault, Kalgoorlie Terrane. Hosts the Genesis and New Holland gold deposits, and with the Claudius Formation, hosts the Waroonga (Emu) gold deposit.|2664 +/- 5 Ma (maximum depositional age).||||Metasedimentary rocks (fine-grained and quartz-rich mica schists) including siltstone and quartz-rich, well-sorted, coarse- to medium-grained sandstone. Locally pervasively deformed.|
31033|Scotty Creek Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2662 - 2640 Ma (inferred).||Includes Claudius Member||Conglomerate, fine to medium grained arkosic sandstone, sandstone and siltstone; metamorphosed.|
31033|Scotty Creek Formation|70326|4|Described|p337,339|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton. Thickness: 1500m. In unconformably fault contact with underlying ultramafic-mafic stratigraphy. Max depositional age from Dunphy et al., 2003; Squire et al., 2010.|Max dep age of 2664+\-5 Ma||Includes Claudius Member.|Correlable to Kurrawang Group.|Polymictic conglomerate and quartzo-feldspathic sandstones.|
31033|Scotty Creek Formation|71212|4|Described|intro p2, intro p3, p28|Neoarchean|Neoarchean|Yilgarn Craton. Equivalent to the informal Scotty Creek metasediments. Contains more than 75 percent of the gold mineralisation of the Lawlers region within shears and vein stockworks. Deposited in a deltaic environment. |2662 +/- 5 Ma||Includes the Claudius Member.||Mature sandstones.|
31033|Scotty Creek Formation|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma); Yilgarn Craton events (4000 - 2600 Ma). See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv.|2662+\-5 Ma; 2640 Ma||Includes Claudius Member.||Sandstone: arkosic, fine to medium-grained, rare pebbles, metamorphosed; siltstone, conglomerate; metamorphosed.|
31033|Scotty Creek Formation|71310|6|Mentioned|p776|||Aoukar and Whelan (1990). Subsequently the Jones Creek Conglomerate.||||||
31033|Scotty Creek Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||Max age 2662+/-5 Ma, min ~2640 Ma.||||Arkosic sandstone with subordinate conglomerate; metamorphosed.|
31033|Scotty Creek Formation|72049|5|Briefly described|p256, p259|||Geochronology analyses, results, and interpretation are discussed in detail. Referred to as the Scotty Creek Sandstone on p261.|2658-2655 Ma|Kurrawang Group|||Quartz-rich volcanic sandstone with minor felsic volcanic conglomerate.|
31033|Scotty Creek Formation|73151|4|Described|p1, p4 Fig.2, p5-7, p9 Fig.5, p11-16|Neoarchean|Neoarchean|Yilgarn Craton, Kalgoorlie Terrane. Approx 1000-1500 m thick. Also referred to as the Jones Creek Formation (Aouker and Whelan, 1990). Disconformably above the Mount White Group, contact has been interpreted as an unconformity but is partly faulted by the Emu Shear Zone. Pebbly sandstones bearing chert clasts are locally known as the Edmunds Facies (informal). 2662 +/- 5 Ma SHRIMP detrital zircon maximum depositional age from Dunphy et al., (2003). Conglomerate clasts are derived from upper half of the Kalgoorlie Group down to the Agnew Komatiite and Never Can Tell Basalt, felsic clasts are dominantly plutonic. Depositional environment of a braided river, upper- and lower-flow regimes with mass flow processes, post-magmatic. Volumetrically minor siltstones near the centre of the basin represent turbidites and a locally subaqueous environment. Equivalent to the Scotty Creek Sequence?|ca. 2665-2655 Ma, 2662 +/- 5 Ma SHRIMP zircon||Claudius Member|Unconformably overlies Kalgoorlie Group, Redeemer Basalt, Redeemer Dolerite, Maria Mine Formation.|Massive, bedded and cross-bedded sandstone, Includes a basal conglomerate and pebbly sandstones containing chert clasts. Conglomerate contains many rounded felsic plutonic clasts, is massive, poorly sorted, clast-supported with a sandy matrix.|
31033|Scotty Creek Formation|73238|5|Briefly described|p5, 12, 13 Fig.10, 27|||Agnew district, Eastern Goldfields Terrane.|2662 +/- 5 Ma (MDA: Dunphy et al., 2003).|||||
31033|Scotty Creek Formation|73596|5|Briefly described|p1152, 1154, 1157-1162, 1169|Neoarchean|Neoarchean|Lawlers Dome, Agnew-Wiluna Greenstone Belt. Source-proximal alluvial fan deposits (conglomerate clasts sourced from Two Sisters Subgroup and Turret Dolerite). Inherited zircons aged between 2820 and 2810 Ma.|2662 +/- 5 Ma (MDA).|||Overlies Maria Mine Formation (Mount White Group); unconformably overlies Turret Dolerite. Is faulted against Two Sisters Subgroup (to the E) and Waroonga Gneiss (to the W).|Basal polymict conglomerate, overlain by pebbly sandstones and minor siltstones.|
32582|Scrubber Granite|23485|4|Described|p23|Mesoproterozoic|Paleoproterozoic|Of Moorarie Supersuite.  Age: 1796 +/- 6Ma, 2290 +/- 11Ma (SHRIMP U-Pb).||||||07-NOV-08
32582|Scrubber Granite|23486|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Moorarie Supersuite. Geological Province: Gascoyne Complex.||||||07-NOV-08
32582|Scrubber Granite|23525|4|Described|p23|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Complex||||||07-NOV-08
32582|Scrubber Granite|23527|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Moorarie Supersuite, Gascoyne Complex||||||07-NOV-08
32582|Scrubber Granite|23780|5|Briefly described|p28|Paleoproterozoic|Paleoproterozoic|Age: ~1800+/-7 Ma||||||07-NOV-08
32582|Scrubber Granite|23781|5|Briefly described|p44 Fig. 19|Paleoproterozoic|Paleoproterozoic|Of Moorarie Supersuite.||||||07-NOV-08
32582|Scrubber Granite|24544|4|Described|p10 Tb.1|Paleoproterozoic|Paleoproterozoic|Age: c. 1800 Ma. Of Moorarie Supersuite. Intrudes Halfway Gneiss.||||||07-NOV-08
32582|Scrubber Granite|50218|5|Briefly described|p240 Fig.2|Paleoproterozoic|Paleoproterozoic|Of the Moorarie Supersuite. Age: c.1800Ma. Geological Province: Gascoyne Complex.||||||07-FEB-11
32582|Scrubber Granite|50219|5|Briefly described|p260 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Moorarie Supersuite.  Age: c.1800Ma.  Geological Province: Gascoyne Complex.||||||07-FEB-11
32582|Scrubber Granite|63866|5|Briefly described|p157|Statherian|Orosirian|Glenburgh Terrane.Age is a SHRIMP date derived from Occhipinti and Sheppard, 2001.|1796 +/-6 Ma |Moorarie Supersuite|||Granite and pegmatite.|
32582|Scrubber Granite|66110|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Moorarie Supersuite. Biotite(-tourmaline) monzogranite, fine- to medium-grained, equigranular, commonly with abundant clusters of tourmaline; locally nodular texture; massive to weakly foliated.||||||
32582|Scrubber Granite|66299|4|Described|p10, pp149-150.|Paleoproterozoic|Paleoproterozoic|Mooloo Zone, southern Gascoyne Province. Forms several sheet-like intrusions, dykes, plugs and veins.|1800 +/- 7 Ma to 1796 +/- 6 Ma.|Unit in Moorarie Supersuite.||Intrudes Dumbie Granodiorite, Halfway Gneiss and Moogie Metamorphics. Faulted contact with Edmund Group siltstone. Unconformably overlain by Mount James Subgroup.|Biotite-muscovite(-tourmaline) monzogranite, fine- to medium-grained, equigranular, commonly with abundant clusters of tourmaline; locally nodular texture; massive to weakly foliated.|
32582|Scrubber Granite|66579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Unit in Moorarie Supersuite.|||Biotite(-tourmaline) monzogranite, fine- to medium-grained, equigranular, commonly with abundant clusters of tourmaline; locally nodular texture; massive to weakly foliated.|
32582|Scrubber Granite|66950|6|Mentioned|p21|||||||||
32582|Scrubber Granite|67247|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|1817 - 1776 Ma.|Unit in Moorarie Supersuite.|||Fine- to medium-grained, equigranular, biotite (tourmaline) monzogranite; commonly with abundant clusters of tourmaline; locally nodular texture; massive to weakly foliated.|
32582|Scrubber Granite|67371|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.||Unit in Moorarie Supersuite.|||Porphyritic to equigranular, coarse-grained, biotite- and muscovite-bearing monzogranite, syenogranite, and pegmatite; locally tourmaline bearing.|
32582|Scrubber Granite|67843|5|Briefly described|p13.|Paleoproterozoic|Paleoproterozoic|Mooloo Zone.|c.1800 Ma.|||||
32582|Scrubber Granite|68521|5|Briefly described|Map Legend|Statherian|Orosirian|Geochronology by Evans et al. (2003).|c.1830-1780 Ma|Of the Moorarie Supersuite.|||Biotite(-tourmaline) monzogranite, fine- to medium-grained, equigranular, commonly with abundant clusters of tourmaline; locally nodular texture; massive to weakly foliated.|
32582|Scrubber Granite|68522|5|Briefly described|Map Legend|Statherian|Orosirian|Gascoyne Province. |1820-1775 Ma|Of the Moorarie Supersuite.|||Biotite(-tourmaline) monzogranite, fine- to medium-grained, equigranular, commonly with abundant clusters of tourmaline; locally nodular texture; massive to weakly foliated.|
32582|Scrubber Granite|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Age fromn sample of monzogranite (168939.1.pdf)|1800 Ma +/- 7 Ma (SHRIMP)|Moorarie Supersuite|||Biotite(--tourmaline) monzogranite; fine- to medium-grained, equigranular, commonly with abundant clusters of tourmaline; locally nodular texture; massive to weakly foliated|
32582|Scrubber Granite|70375|6|Mentioned|p818 fig. 1, p826|Paleoproterozoic|Paleoproterozoic|Shown as a mineral deposit p818 and as informal Scrubber granite and Scrubber Granites p826. Potential source of tourmaline in Tumblagooda Sandstone.|||||Granite.|
32582|Scrubber Granite|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_geologyl_lut.csv, 100k_interpgeop_lut.csv, 168939.1.pdf|1800-1796 Ma|||Intrudes Dalgaringa Supersuite, Dumbie Granodiorite|Biotite(-tourmaline) monzogranite, fine- to medium-grained, equigranular, commonly with abundant clusters of tourmaline; locally nodular texture; massive to weakly foliated.|
32582|Scrubber Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
32582|Scrubber Granite|71869|5|Briefly described|p6, app p6|||Capricorn Orogen.|1800 Ma, 1796 +/- 6 Ma (cryst.)|Moorarie Supersuite|||Biotite monzogranite.|
78608|Scrubby Tank Gabbro|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||2960 - 2650 Ma (inferred).||||Gabbro; metamorphosed.|
78608|Scrubby Tank Gabbro|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2960-2650 Ma (inferred)||||Gabbro; metamorphosed|
29212|Scrutons Monzogranite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1860Ma. Geological province: Kimberley Province (West).||||||07-FEB-11
29212|Scrutons Monzogranite|42710|5|Briefly described|map legend|Proterozoic||||||||
29212|Scrutons Monzogranite|42811|5|Briefly described|p12|||||||||
29212|Scrutons Monzogranite|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|Approx 1865 - 1850 Ma.||||||
29212|Scrutons Monzogranite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite.||||||07-NOV-08
29212|Scrutons Monzogranite|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province; Halls Creek Orogen; North Australian Craton.||Paperbark Supersuite.|||Porphyritic biotite metamonzogranite.|
29212|Scrutons Monzogranite|70154|5|Briefly described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic||1852-1864 Ma|Paperbark Supersuite|||Porphyritic biotite metamonzogranite.|
29212|Scrutons Monzogranite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 100k_geologyp_lut.csv.|1864-1852 Ma (inferred)|Unit of Paperbark Supersuite.|||Coarse porphyritic biotite monzogranite, partly recrystallised or chloritised in places|
29212|Scrutons Monzogranite|72437|6|Mentioned|p65, p71|||Hooper Complex. Whole-rock analyses are provided.||Paperbark Supersuite||||
78986|Scuddles Member|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton.|c.2962 Ma.|Gossan Hill Formation.|||Porphyritic dacite with lesser rhyodacite and felsic volcaniclastic units; locally with economic sulfide mineralisation; metamorphosed.|
78986|Scuddles Member|70796|5|Briefly described|100k_geologyp_lut.csv|Mesoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. See also 100K_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 155879.1.pdf, 203702.1.pdf, 203703.1.pdf, 203704.1.pdf, Badja100_2240_stratig.pdf. Numerous additional lithologies are discussed.|2958 +/ 6 Ma (isotopic)|Gossan Hill Formation||Overlies the Golden Grove and Gossan Valley members.|Porphyritic dacite with lesser rhyodacite and felsic volcaniclastic units; locally with economic sulphide mineralization; metamorphosed|
78986|Scuddles Member|71269|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). Sample GSWA 203702 (metadacite) yielded a weighted mean 207Pb/206Pb date of 2962+\-4 Ma, interpreted as the magmatic crystallization age of the dacite. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv.|2958+\-6 Ma|Unit of Gossan Hill Formation.||Underlain by Golden Grove and Gossan Valley members. Intruded by Gnows Nest Granodioite.|Porphyritic dacite with lesser rhyodacite and felsic volcaniclastic units; locally with economic sulphide mineralization; metamorphosed|
78986|Scuddles Member|71272|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c.2958 Ma.|Gossan Hill Formation.|||Porphyritic dacite with lesser rhyodacite and felsic volcaniclastic units; locally with economic sulfide mineralisation; metamorphosed.|
72566|Scutellid Bed|62735|5|Briefly described|p982|Frasnian|Frasnian|Informally named horizon within Virgin Hills Formation containing rich macrofossil assemblages; trilobites. Geol. Prov: Canning Basin.||||||
78628|Seabrook Intrusion|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton|||Includes 3 unnamed subunits.||Peridotite, commonly altered to a talc-carbonate assemblage; cumulate texture; pyroxenite, gradational contact with overlying gabbro; gabbro with subordinate pyroxenite; all metamorphosed.|07-AUG-15
78628|Seabrook Intrusion|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Peridotite, commonly altered to a talc-carbonate assemblage; cumulate texture. Pyroxenite with gradational contact with overlying gabbro. Gabbro with subordinate pyroxenite. All metamorphosed.|
78628|Seabrook Intrusion|71270|4|Described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton.|||||Peridotite, commonly altered to a talc-carbonate assemblage; cumulate texture; metamorphosed; pyroxenite and gabbro; metamorphosed.|
70716|Seecliff Sandstone|62453|5|Briefly described|p12 Fig. 8|Ediacaran|Ediacaran|Geological Province: Adeliade Rift Complex/Stuart Shelf.||||||
79006|Seeligson Monzogranite|71809|5|Briefly described|map legend|Archean|Archean|Yilgarn Craton||Of Walganna Suite.|||Equigranular, coarse-grained, undeformed monzogranite with 4-12 mm grain size; locally with 3 cm long K-feldspar megacrysts; metamorphosed.|
79006|Seeligson Monzogranite|73023|5|Briefly described|p2-4, 15|||||Bald Rock Supersuite.||Intrudes Mougooderra Formation.||
78854|Selby Granite|66468|6|Mentioned|p17-18 Figs.3,5; p20; p25-26 Figs.8,9|Paleoproterozoic|Paleoproterozoic|Lack of negative gravity anomaly suggests this unit is thin. Highly magnetic.||||||
78854|Selby Granite|69253|5|Briefly described|p759, p760-762 Fig.14,16-17,|||Petrophysical properties described.||Unit in Frederick Suite.||Intrudes Dead Bullock and Killi Killi Formations.||
33996|Semaphore Sand Member|22525|6|Mentioned|p37.41||Holocene|||||||
33996|Semaphore Sand Member|23489|5|Briefly described|p43 Table 1|Holocene|Holocene|||||||
33996|Semaphore Sand Member|60953|5|Briefly described|Map Legend|Holocene|Holocene|White calcareous and siliceous coastal dune sand.||||||
33996|Semaphore Sand Member|60958|5|Briefly described|Map Legend|Holocene|Holocene|Of the Saint Kilda Formation.  Unconsolidated, white bioclastic quartz-carbonate sand of modern beaches and transgressive dune fields.||||||
33996|Semaphore Sand Member|61070|5|Briefly described|Map Legend|Holocene|Holocene|Foredune and dune sand. White to cream quartz and shelly sand. Includes calcareous sand reworked from the Bridgewater Formation and modern beach facies. Of the Saint Kilda Formation.||||||12-JAN-10
33996|Semaphore Sand Member|61108|5|Briefly described|map legend|Holocene|Holocene|White calcareous and siliceous coastal dune sand.||||||
33996|Semaphore Sand Member|61121|5|Briefly described|Map legend|Holocene|Holocene|Of the Saint Kilda Formation. Unconsolidated, white bioclastic quartz-carbonate sand of modern beaches and transgressive dune fields.||||||
33996|Semaphore Sand Member|64282|5|Briefly described|Map legend|Holocene|Holocene|Of the Saint Kilda Formation. Unconsolidated white, bioclastic quartz carbonate sand of modern beaches and transgressive dune fields.||||||
33996|Semaphore Sand Member|65375|5|Briefly described|p42.|Holocene|Holocene|||Unit in Saint Kilda Formation.|||Modern beach and dune sand deposit.|
33996|Semaphore Sand Member|67117|5|Briefly described|Map legend.|Holocene|Holocene||||||Unconsolidated white bioclastic quartz-carbonate sand of modern beaches and transgressive dune fields.|
33996|Semaphore Sand Member|68131|6|Mentioned|p7, p12, p17, p31, p42, p66, p71|Holocene|Holocene|Yorke Peninsula. Appears as Semaphore Sand on p42.||||||
33996|Semaphore Sand Member|69048|5|Briefly described|p2|Cenozoic|Cenozoic|Southern Eyre Peninsula.||Saint Kilda Formation.||||
33996|Semaphore Sand Member|69372|6|Mentioned|p28 Fig.6, p34 fig. 12|Holocene|Holocene|||||||
33996|Semaphore Sand Member|70333|5|Briefly described|Map legend.|Holocene|Holocene||||||Unconsolidated white bioclastic quartz-carbonate sand of modern beaches and transgressive dune fields.|
33996|Semaphore Sand Member|70334|6|Mentioned|p72|||Modern beach sand along the present shoreline and stranded beach ridges within the present supratidal zone.||||||
33996|Semaphore Sand Member|70337|5|Briefly described|Map legend.|Holocene|Holocene||||||Unconsolidated white bioclastic quartz-carbonate sand of modern beaches and transgressive dune fields.|
33996|Semaphore Sand Member|70382|5|Briefly described|p29 Fig 3|Holocene|Holocene|Yorke Peninsula region.|||||Unconsolidated sand|
33996|Semaphore Sand Member|70660|5|Briefly described|p10|Holocene|Holocene|||||||
33996|Semaphore Sand Member|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sand, eolian, beach sediments, coastal sedient|
33996|Semaphore Sand Member|72450|6|Mentioned|Brochure, Brochure map|Holocene|Holocene|Largest deposits occur south of Seaford near the mouth of Pedler Creek and in Aldinga Scrub Reserve at Silver Sands.|||||Beach sand, back-beach dune sand and inland sand drift.|
33996|Semaphore Sand Member|73103|5|Briefly described|Map legend.|Holocene|Holocene||||||Unconsolidated white bioclastic quartz-carbonate sand of modern beaches and transgressive dune fields.|
33996|Semaphore Sand Member|73107|5|Briefly described|Map legend.|Holocene|Holocene||||||Unconsolidated, white bioclastic quartz-carbonate sand of modern beaches and transgressive dune fields.|
33996|Semaphore Sand Member|73110|5|Briefly described|Map legend.|Holocene|Holocene||||||Unconsolidated white bioclastic quartz-carbonate sand of modern beaches and transgressive dune fields.|
33996|Semaphore Sand Member|73188|5|Briefly described|p320, p335|Holocene|Holocene|St Vincent Basin.||Saint Kilda Formation|||Beach sand.|
33996|Semaphore Sand Member|73236|4|Described|p36, p38, p44|Holocene|Holocene|Coastal sediments; beach and dune sands. Patchily covers the shore platform at Hallett Cove.||Saint Kilda Formation|||Lime-cemented gravel (beachrock); beach gravel of mostly quartzite pebbles to boulders; well-sorted, medium-grained quartz beach sand; well-sorted, medium-grained quartz sand of back beach dunes.|
33843|Sequence HR4-1|22546|4|Described|374|||Of Turee Creek Supersequence (Fig 13). Geol province Turee Creek Basin.||||||
33845|Sequence HR4-2|22546|4|Described|374|||Of Turee Creek Supersequence. Geol province Turee Creek Basin||||||
33850|Sequence HR4-3|22546|4|Described|376|||Of Turee Creek Supersequence. Geol province Turee Creek Basin||||||
33852|Sequence HR4-4|22546|4|Described|377|||Of Turee Creek Supersequence. Geol province Turee Creek Basin||||||
33853|Sequence HR4-5|22546|5|Briefly described|377|||Of Turee Creek Supersequence. Geol province Turee Creek Basin||||||
77926|Seven Mile Sandstone Member|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|The rank of Member was omitted.|2657 - 2640 Ma (inferred).|Kurrawang Formation|||Quartz-rich sandstone; massive to planar bedded; rare pebbly sandstone; rare cross-bedding; metamorphosed.|
28996|Shady Camp Limestone Member|40993|6|Mentioned|Fig.1|||||||||
28996|Shady Camp Limestone Member|41840|4|Described|p43|||||||||
28996|Shady Camp Limestone Member|41864|4|Described|p19|||Formerly Shady Camp Limestone||||||
28996|Shady Camp Limestone Member|41865|5|Briefly described|Map legend|Middle Cambrian||||||||
28996|Shady Camp Limestone Member|41866|5|Briefly described|Map legend|Middle Cambrian||||||||
28996|Shady Camp Limestone Member|42070|6|Mentioned|p4|||||||||
28996|Shady Camp Limestone Member|44230|5|Briefly described|Map Legend||Middle Cambrian|||||||
28996|Shady Camp Limestone Member|44868|5|Briefly described|Map Legend|Boomerangian|Ordian|||||||
28996|Shady Camp Limestone Member|60419|4|Described|p1, p3 Fig.2|Middle Cambrian|Middle Cambrian|Of Panton Formation. Max. thickness: 4 m. Shale, marl, marly limestone and limestone. Fossiliferous. Marine. Contains fauna of Ordian age. Geological Province: Ord Basin.||||||
28996|Shady Camp Limestone Member|60589|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Panton Formation (Negri Subgroup, Goose Hole Group).  Grey, stromatolitic fossiliferous and oncoid limestone.  Geological Province: Ord Basin.||||||24-NOV-04
28996|Shady Camp Limestone Member|62789|5|Briefly described|p133|Cambrian|Cambrian|Ord Basin. Contains Xystridura negrina assemblage of moderate diversity including trilobites, brachiopods, hyoliths, molluscs, adrioasteroid ossicles and a ptychoparioid.||Unit in Panton Formation.||||28-MAR-12
28996|Shady Camp Limestone Member|67860|5|Briefly described|p419 Tb. 4-18|Cambrian|Cambrian|0-4 m thick. Type section details given. Fossiliferous: as for Panton Formation.||Panton Formation|||Skeletal, oncolitic limestone.|
28996|Shady Camp Limestone Member|69448|5|Briefly described|p33:2-4; 33:5 Fig.33.7; 33:6|Middle Cambrian|Middle Cambrian|Ord Basin. Intertidal to shallow subtidal deposits. 3-4m thick.||Panton Formation.|||Basal gypsiferous microbial laminite overlain by oncoid-rich nodular hyolith floatstone.|12-JUL-16
28996|Shady Camp Limestone Member|69673|6|Mentioned|p193|||||||||
28996|Shady Camp Limestone Member|71800|5|Briefly described|p26 fig 3|Cambrian|Cambrian|Ord Basin.||Panton Formation||||
79162|Shanes Dam Conglomerate|70772|4|Described|p4-5, p7-9, p11|Cretaceous|Mesoproterozoic|Madura Shelf. Localised to four wells; HDDH001, HDDH002, SDDH001 and SDDH002 wherein the unit attains thicknesses of 25m, >1m, 24m and 4m respectively. This unit is highly magnetic in its geophysical response. An age could not be derived from palynology. Deposited in a high-energy, alluvial to fluvial type setting with localised steep topography able to transport and round cobbles and pebbles. See also p17, p22, p24, p28, p31, p34, p39, p41.|c. 1410 Ma|||Disconformably overlain by the Madura Formation.|Rounded quartz, sandstone, mafic and granitic, pebble cobble conglomerate that is clast supported, moderate to well consolidated with variable carbonate cement.|
79162|Shanes Dam Conglomerate|71618|4|Described|p122,124-130,132-133,135,137|Cretaceous|Devonian|Geological province: ?Officer Basin or older. Present in 4 cores: HDDH001, HDDH002, SDDH001 and SDDH002. Thickness: <1-25m. Depositional environment: high energy, alluvial-fluvial. U-Pb ICPMS zircon analysis yield a single-well-defined concordant c. 1412 Ma peak (likely from underlying Haig Cave Supersuite). Zircon provenance from underlying Haig Cave Supersuite indicates local sediment sourcing from underlying crystalline basement and potential intermediate sedimentary packages. Single concordant Devonian zircon (407 Ma) also present as an outlier, but may represent a maximum depositional age. Otherwise, depositional age is temporally constrained by the next youngest concordant zircon age subgroup at 1301 Ma (1300+\-15 Ma; 1302+\-16 Ma).||||Overlain disconformably by Madura Formation. Underlain unconformably by Madura Province crystalline basement.|High ferruginised conglomerate: oligo- to polymict, with typically well rounded sandstone, soft green and white claystone, vein quartz, mafic and gneissic/granitic clasts identifiable.|06-SEP-19
79162|Shanes Dam Conglomerate|73084|5|Briefly described|p16-18|Ectasian|Calymmian|Intersected in drillhole HDDH001 (Reynolds, 2016). Disconformably underlies Cretaceous sequence. Age is a maximum depositional age where a major detrital zircon age component was identified at c. 1400 Ma, which matches the age of the underlying Haig Cave Supersuite [may not be close to the true depositional age].|c. 1400 Ma [see comments]|||Underlain by Haig Cave Supersuite [basement rocks]. Overlain by Madura Formation.||
32780|Shay Intrusion|23415|5|Briefly described|Map Legend|Archean|Archean|Geological province:  Pilbara Craton.  Metamorphosed gabbro, epidotised gabbro and quartz gabbro.||||||07-NOV-08
32780|Shay Intrusion|23757|5|Briefly described|p10, p13|||Layered mafic rocks - basal ultramafic pyroxenite successively overlain by norite, gabbronorite, gabbro and quartz gabbro layers.||||||07-JAN-08
32780|Shay Intrusion|44229|5|Briefly described|Map Legend|Archean|Archean|In the Pilbara Supergroup.||||||07-NOV-08
32780|Shay Intrusion|60429|2|Defined|p18, p37 Appx.1|Archean|Archean|Intrudes contact between Cooieena Basalt (Gorge Ck Gp) and Cattle Well Fm. Age: <3048Ma. Max. thickness: 500m. Thick norite body, sill-like, layered, at least 100km long. Epidotized quartz gabbro, gabbro-norite, pyroxenite; weakly metamorphosed.||||||07-FEB-11
32780|Shay Intrusion|63441|5|Briefly described|p13 Tb. 2|Archean|Archean|Geological province: East Pilbara Terrane. On SHAY GAP map sheet.||||||07-FEB-11
32780|Shay Intrusion|64580|4|Described|map legend||Mesoarchean|Of Dalton Suite. Gabbro, norite, and pyroxenite.||||||15-DEC-08
32780|Shay Intrusion|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|Age derived from sample of felsic granophyric igneous rock (180056.1.pdf)|3006 +/-7 Ma (SHRIMP)|Sisters Supersuite|||Metagabbro, epidotized metagabbro, metamorphosed quartz gabbro, metamorphosed gabbronorite, norite and pyroxenite.|
32780|Shay Intrusion|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.||Unit of Dalton Suite.|||Gabbro, norite, and pyroxenite|
32780|Shay Intrusion|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||gabbro, quartz gabbro, gabbronorite, norite|
32780|Shay Intrusion|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|De Grey Superbasin.||Langenbeck Suite|||Gabbro, norite, and pyroxenite; metamorphosed.|
31895|Shepherds Bore Granite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  Age: c. 1835-1805 Ma.||||||07-NOV-08
31895|Shepherds Bore Granite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs Supersuite. Age: 1825Ma. Geological province: Kimberley Province.||||||07-FEB-11
31895|Shepherds Bore Granite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  In the Bow River batholith.  Age: 1835-1805Ma.||||||07-NOV-08
31895|Shepherds Bore Granite|43854|5|Briefly described|Map Legend||Proterozoic|Sally Downs supersuite.||||||
31895|Shepherds Bore Granite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31895|Shepherds Bore Granite|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Sally Downs Supersuite.||||||07-NOV-08
31895|Shepherds Bore Granite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Kevins Dam Suite|||Weakly porphyritic, biotite monzogranite and syenogranite.|04-AUG-15
31895|Shepherds Bore Granite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Kevins Dam Suite|||Weakly porphyritic, biotite monzogranite and syenogranite.|
31895|Shepherds Bore Granite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2.|1827-1808 Ma (Inferred)|Unit of Kevins Dam Suite.|||Weakly porphyritic, biotite monzogranite and syenogranite|
31895|Shepherds Bore Granite|70154|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1808-1827 Ma|Kevins Dam Suite|||Weakly porphyritic, biotite monzogranite and syenogranite|
31895|Shepherds Bore Granite|71267|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma).|1827-1808 Ma (inferred)|Unit of Kevins Dam Suite.|||Weakly porphyritic, biotite monzogranite and syenogranite|
31895|Shepherds Bore Granite|72437|5|Briefly described|p102, p104-105|||Whole rock analyses are provided.||Kevins Dam Suite|||Biotite monzogranite, granodiorite, biotite syenogranite.|
38617|Sherlock Bay Complex|23784|5|Briefly described|p12|Archean|Archean|||||||07-NOV-08
38617|Sherlock Bay Complex|70312|6|Mentioned|p2|||West Pilbara Block.||||Abuts Caines Well Granite.|Granophyre.|
37207|Sherlock Intrusion|23793|5|Briefly described|p30|||||||||
37207|Sherlock Intrusion|24024|5|Briefly described|Map Legend|Archean|Archean|Informal name - structural term, not stratigraphic. Of the Pilbara Supergroup. Geological Province: Pilbara Craton.||||||15-DEC-08
37207|Sherlock Intrusion|24189|5|Briefly described|p802 Fig.1, p803|Archean|Archean|Age: 2925 Ma. Geological Province: Mallina basin.||||||15-DEC-08
37207|Sherlock Intrusion|24190|6|Mentioned|p820 Fig.1|||||||||
37207|Sherlock Intrusion|24550|6|Mentioned|p39|||Informal name. Intrudes Caines Well Granitoid Complex. See also p81 Fig. 5.4.||||||07-FEB-11
37207|Sherlock Intrusion|63441|5|Briefly described|p12 Tb. 2, p38|Archean|Archean|Of the Radley Suite. A major sill which outcrops discontinuously across an area of 1000sq.km. mafic layered intrusion. Locally over 1km thick. Age: 2925+/-4Ma. Geological Province: West Pilbara Superterrane.||||||07-FEB-11
37207|Sherlock Intrusion|64174|5|Briefly described|Map legend|Archean|Archean|Part of the Radley Suite (Sisters Supersuite). Gabbro and minor pyroxenite and granophyre; metamorphosed.||||||07-NOV-08
37207|Sherlock Intrusion|64580|4|Described|map legend||Mesoarchean|Of Radley Suite. Gabbro, and minor pyroxenite and granophyre; metamorphosed.||||||15-DEC-08
37207|Sherlock Intrusion|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological Province: West Pilbara Granite-Greenstone Terrane, Central Pilbara Tectonic Zone, and southwest Pilbara inlier, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 2925 Ma|Unit of Radley Suite.|||Gabbro, and minor pyroxenite and granophyre; metamorphosed|
37207|Sherlock Intrusion|69300|5|Briefly described|map legend|Archean|Archean|West Pilbara Granite-Greenstone Terrane||Pilbara Supergroup|||undivided gabbro, mafic, and ultramafic rocks forming layered sills; metamorphosed|
37207|Sherlock Intrusion|70775|5|Briefly described|p64-p66, p77|Mesoarchean|Mesoarchean|Locally over 1km thick and intrudes along the contact between the Caines Well Granitic Complex and the Whim Creek Group.|c. 2950 Ma|Langenbeck Suite||Overlain by the Bookingarra Group.||
37207|Sherlock Intrusion|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||olivine gabbro, granophyre|
37207|Sherlock Intrusion|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Langenbeck Suite|||Gabbro, and minor pyroxenite and granophyre; metamorphosed.|
70641|Shilliman Monzogranite|61252|5|Briefly described|p67 Tb.1|Archean|Archean|Age: 2930+/-3 Ma. Of the Carlindi granitoid complex.||||||07-NOV-08
79382|Shingle Creek Group|70795|5|Briefly described|2_5m_interpgeop15_lut.csv|Paleoproterozoic|Paleoproterozoic||2208 Ma||||Conglomerate, sandstone, mudstone, basalt and chert.|
79382|Shingle Creek Group|70814|5|Briefly described|p4, p32, p34-p35, p70|Paleoproterozoic|Paleoproterozoic|Formerly the Lower Wyloo Group.|c. 2208 Ma||Includes the Beasley River Quartzite.|||
79382|Shingle Creek Group|70826|6|Mentioned|p6 tbl 2, p9|Paleoproterozoic|Paleoproterozoic|Turee Creek Basin. Formerly known as the lower Wyloo Group. Probably a time equivalent to the Moogie Metamorphics.||||Unconformably overlies the Turee Creek Group.||
79382|Shingle Creek Group|70949|5|Briefly described|p988-989, p998-1000|Paleoproterozoic|Paleoproterozoic|Formerly the lower Wyloo Group. Deposited during the 2215-2145 Ma Ophthalmian Orogeny. Up to ~3 km thick.|||Beasley River Quartzite, Cheela Springs Basalt.|Is overlain by the Wyloo Group.|Conglomerate, sandstone, mudstone, basalt, chert and locally stroamtolitic dolomite; intruded by dolerite dykes and sills.|
79382|Shingle Creek Group|71513|6|Mentioned|p66 fig 1,|||Pilbara Craton.||||||
79382|Shingle Creek Group|71803|6|Mentioned|p367 fig 1|||||||||
79382|Shingle Creek Group|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Turee Creek Basin.|||Includes Cheela Springs Basalt, Beasley River Quartzite.|Intruded by Balgara Dolerite sills.|Basalt and mafic volcaniclastic rock; sandstone, conglomerate, pebbly sandstone, and siltstone; intruded by Balgara Dolerite sills.|
79382|Shingle Creek Group|72570|6|Mentioned|p2-p3||||||Includes the Beasley River Quartzite and the Cheela Springs Basalt.|Unconformably overlies the Turee Creek Group.||
79382|Shingle Creek Group|72712|5|Briefly described|p1-2, p9, p23, p25, p29-32, p42, p43, 49|Rhyacian|Rhyacian|New Name. See also p50, p53, p56. Much of the formerly named 'lower Wyloo Group' is now included in this group, but the 'Wooly Dolomite' has been excluded and renamed Wooly Formation. Folding of this group is constrained to >2008 Ma by undeformed Panhandle Dolerite.|c.> 2208 +/- 10 Ma.||Includes Beasley River Quartzite, Cheela Springs Basalt.|Shown as unconformably overlying Turee Creek Group and underlying Capricorn Group. Intruded by Balgara Dolerite. Faulted against the Wyloo Group.|Includes sandstone, conglomerate, basalt.|14-JAN-21
79382|Shingle Creek Group|73022|6|Mentioned|p2 Fig.1|||||||||
79382|Shingle Creek Group|73290|6|Mentioned|p784|||Hamersley Province.||||||
22841|Shoonta Hill Sand|64449|2|Defined|p75, p79 Tb. 5, p81-83|Holocene|Holocene|Overlies; Cable Beach Sand (gradational), Mowanjun Sand (sharpe contact), Church Hill Sand, Barn Hill Formation. Age: 1190+/-170 yrs BP, 2440+/-190 yrs BP. Thick: 8m. White fine-grained sand; shoe-string to lensoid deposit formed as supratidal dunes.||||||07-FEB-11
22841|Shoonta Hill Sand|73213|5|Briefly described|955, 956 Fig.1, 958 Fig.3, 959, 961|||Forms coastal or inland-ingressing dunes. Derived from the Mowanjum Sand. See also p963-965 Figs.11-13, 967-968.||||Overlies Mowanjum Sand and Cable Beach Sand.|White quartz sand. Contains shell middens.|
23966|Shotts Formation|14227|5|Briefly described|Enclos. 2|Early Permian|Early Permian|Of the Stockton Group. Underlies Moorhead Formation. Presented as Shotts only.||||||07-FEB-11
23966|Shotts Formation|22820|6|Mentioned|p13|||Of the Stockton Group. Previously mapped as the diamictite part of the former Stockton Formation.||||||12-AUG-08
23966|Shotts Formation|23174|5|Briefly described|Fig5p8|Early Permian|Early Permian|||||||
23966|Shotts Formation|42711|2|Defined|p5 Fig. 5, p19,  Plates 2, 4|Early Permian|Late Carboniferous|Of Stockton Group, replacing Stockton Fm within the group. Unconformable below Moorhead Fm. Geol.prov: Collie Basin. Diamictite/tillite mainly.  Correlations presented.||||||29-APR-09
23966|Shotts Formation|43442|6|Mentioned|p50|||||||||
23966|Shotts Formation|64630|5|Briefly described|p31 Fig.2|Asseliean|Gzhelian|Province: Collie Subbasin. Underlies the Moorehead Formation. Palynology age: D. tenuistriatus. Top correlates with the top of the Cullens Diamictite. Parent: Stockton Group. Inferred glacial influence.||||||18-JAN-10
23966|Shotts Formation|70097|5|Briefly described|p19 Fig.3|Asselian|Asselian|Southern Perth Basin. Collie Sub-basin.||Stockton Group||Is overlain by Moorhead Formation.|Sandstone.|12-SEP-17
23966|Shotts Formation|70774|5|Briefly described|p5 fig 3|Asselian|Asselian|Collie Basin.||Stockton Group||Overlain by the Moorehead Formation.||
41173|Siffleetes Granodiorite|50379|5|Briefly described|Map Legend|Archean|Archean|Part of Yule Granitoid Complex. Geological Province: Pilbara Craton.||||||07-NOV-08
41173|Siffleetes Granodiorite|63441|5|Briefly described|p9 Tb. 2|Archean|Archean|Of the Cleland Supersuite. Geological province: Pilbara Craton.||||||07-FEB-11
41173|Siffleetes Granodiorite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Cleland Supersuite. Meta biotite-hornblende granodiorite; locally common amphibolite and diorite xenoliths; moderately to strongly foliated.||||||
41173|Siffleetes Granodiorite|69013|5|Briefly described|Map Legend|Paleoarchean||East Pilbara Terrane.||Of the Cleland Supersuite.||Intrudes the Sisters Supersuite.|Meta biotite-hornblende granodiorite; locally common amphibolite and diorite xenoliths; moderately to strongly foliated.|29-APR-14
41173|Siffleetes Granodiorite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Cleland Supersuite|||Meta biotite--hornblende granodiorite; locally common amphibolite and diorite xenoliths; moderately to strongly foliated.|
41173|Siffleetes Granodiorite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|3274-3224 Ma (inferred)|Unit of Cleland Supersuite.|||Metamorphosed biotite-hornblende granodiorite; locally common amphibolite and diorite xenoliths; moderately to strongly foliated|
41173|Siffleetes Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite|
41173|Siffleetes Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|||Cleland Supersuite|||Metamorphosed biotite--hornblende granodiorite; locally common amphibolite and diorite xenoliths; moderately to strongly foliated.|
23969|Siggins Spring Member|13194|4|Described|p392 Tb. 4-16|Frasnian|Frasnian|Type Section: eastern Hargreaves Hills 19o55'S 128o40'E. 190m thick fluvial deposits.||Hargreaves Formation (near base)|||Quartz sandstone; minor siltstone.|
23969|Siggins Spring Member|40993|2|Defined|p6|Frasnian|Frasnian|||||||
23969|Siggins Spring Member|41598|6|Mentioned|p413|||||||||
23969|Siggins Spring Member|41864|4|Described|p54|||Previously mapped as Cecil Sandstone||||||
23969|Siggins Spring Member|41865|5|Briefly described|Map legend|Frasnian||||||||
23969|Siggins Spring Member|41867|5|Briefly described|Map legend|Frasnian||||||||
23969|Siggins Spring Member|42030|5|Briefly described|p749|||||||||
23970|Silt Dam Monzogranite|41786|6|Mentioned|Fig.2|||||||||
23970|Silt Dam Monzogranite|42740|5|Briefly described|map legend|Archean||||||||07-NOV-08
23970|Silt Dam Monzogranite|43125|4|Described|p9, and map insert|Archean|Archean|||||||03-MAR-10
23970|Silt Dam Monzogranite|43232|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
23970|Silt Dam Monzogranite|60076|6|Mentioned|p46 App. 1|||[Agmst]   Seriate biotite monzogranite.||||||
23970|Silt Dam Monzogranite|65204|6|Mentioned|p18 Tbl.3.|Neoarchean||2-6mm grains; equigranular||||||
23970|Silt Dam Monzogranite|65264|5|Briefly described|p48 Appdx. 1|Archean|Archean|Seriate biotite monzogranite; marginal zones have contact-parallel foliation with steep mineral lineation.||||||07-FEB-11
23970|Silt Dam Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Seriate biotite monzogranite; marginal zones have contact-parallel foliation with steep mineral lineation.|07-AUG-15
23970|Silt Dam Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Seriate biotite monzogranite; marginal zones have contact-parallel foliation with steep mineral lineation.|
23970|Silt Dam Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
23970|Silt Dam Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|3010-2600 Ma (inferred)||||Seriate biotite monzogranite; marginal zones have contact-parallel foliation with steep mineral lineation|
23972|Silver Lake Member|23130|5|Briefly described|p348|||of Kambalda Komatiite.  Underlies Tripod Hill Member.||||||
23972|Silver Lake Member|24325|5|Briefly described|p58|||Of the Kambalda Komatiite Formation (Kambalda Group). Geological Province: Kambalda Dome, Yilgarn Craton.||||||
23972|Silver Lake Member|41670|5|Briefly described|p249|||||||||
23972|Silver Lake Member|41890|5|Briefly described|Table 1|||||||||
23972|Silver Lake Member|43162|6|Mentioned|17|||||||||
23972|Silver Lake Member|50548|4|Described|p1174||Archean|Experienced significant talc-carbonate alteration. Lower member of Kambalda Komatiite Formation. Overlies Lunnon Basalt, possibly conformably with contact area hosting NiS ore, and underlies Tripod Hill Member.||||||07-FEB-11
23972|Silver Lake Member|60514|5|Briefly described|p28|Archean|Archean|Of the Kambalada Komatiite. Overlain by the Tripod Hill Member. Maximum thickness: 100m. Geological Province: Yilgarn Craton.||||||07-FEB-11
23972|Silver Lake Member|60578|5|Briefly described|p5|Archean|Archean|Of Kambalda Komatiite. 3-6 komatiitic peridotite flows up to 100m thick.||||||07-NOV-08
23972|Silver Lake Member|60623|4|Described|p28|Archean|Archean|Lower member of Kambalda Komatiite. Several, 10-100m thick komatiite flows, in lower cumulate and upper spinifex zones. Overlain by Tripod Hill Member, overlies Lunnon Basalt.||||||07-NOV-08
23972|Silver Lake Member|62110|5|Briefly described|p1442 Fig. 1, p1452|Archean|Archean|Of the Kambalda Komatiite. Hosts nickel ore shoots. Age: 2709+/-4Ma. Geological Province: Kambalda dome in the Norseman-Wiluna greenstone belt, Yilgarn Carton.||||||07-FEB-11
23972|Silver Lake Member|67198|4|Described|p81, p84-87, p89-90.|Neoarchean|Neoarchean|30-200m thick with nickel sulphide mineralisation associated with thickened (>30m) channels. Ortho-mesocumulate textures. Thickened olivine cumulates are also present and are the product of sustained lava flow and continuous olivine accumulation. Geochemistry discussed in detail.|<2702 +/- 4 Ma (maximum depositional age).|Kambalda Komatiite||Overlain by Tripod Hill Member. Is intruded by Kambalda Granodiorite.|Comprises one or more laterally continuous flow units, with interflow sediments intercalated with komatiite flows.|11-SEP-17
23972|Silver Lake Member|68289|5|Briefly described|p6-p7|||Southern Kalgoorlie Terrane. Part of the mafic-ultramafic succession which is overlain by the Black Flag Group. 30-200m thick. Hosts nickel mineralisation.||Kambalda Komatiite||Overlies the Lunnon Basalt. Overlain by the Tripod Hill Member. Intruded by the Kambalda Granodiorite.|Contains thin sulfidic sediments, carbonaceous slaty sediments and minor mafic sediments.|
23972|Silver Lake Member|69583|5|Briefly described|p37|||Southern Kalgoorlie Terrane. 30-200m thick.||Kambalda Komatiite.||||
23972|Silver Lake Member|69631|5|Briefly described|p7, p9|||Kambalda area, Kalgoorlie Terrane. 30-200m thick. Hosts Ni mineralisation.||Kambalda Komatiite.||Overlies Lunnon Basalt. Is overlain by Tripod Hill Member.||
23972|Silver Lake Member|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2709 - 2692 Ma (inferred).|Kambalda Komatiite|||Komatiite, lower unit; pyroxenite; cumulate to spinifex-textured flows 10-100 metre thick; nickel sulphides common; thin intercalated sedimentary units; commonly serpentinized.|
23972|Silver Lake Member|70773|5|Briefly described|p14, p26-p27|||40-100m thick.||Kambalda Komatiite||Overlies the Lunnon Basalt.|Spinifex textured komatiitic rocks.|
23972|Silver Lake Member|70863|6|Mentioned|p6, 12|||Kalgoorlie Terrane. Shows no significant chalcophile element anomalies beyond the immediate deposit scale. Also appears as Lower Silver Lake komatiites.||Kambalda Komatiite Formation.||||
23972|Silver Lake Member|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2709+\-4 Ma; 2692+\-4 Ma|Unit of Kambalda Komatiite.|||Komatiite, lower unit; pyroxenite; cumulate to spinifex-textured flows 10--100 metre thick; nickel sulfides common; thin intercalated sedimentary units; commonly serpentinized|
80614|Singleton Formation|71809|5|Briefly described|map legend|Mesoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane||Of Norie Group|||Psammitic and pelitic schist interlayered; metabasalt; metamorphosed ultramafic rock;serpentinized metaperidotite; interlayered pillow lava + hyaloclastite, siltstone; pyroxene spinifex-textured basalt.|06-SEP-19
80614|Singleton Formation|72389|5|Briefly described|Map Legend|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Gabanintha 1:100k map sheet 2644. Includes numerous unnamed constituents.||Norie Group|Includes the Quinns Basalt Member.||Fine-grained, mafic amphibolite schist. Metakomatiitic basalt, pillowed basalt.|28-AUG-20
80614|Singleton Formation|72494|5|Briefly described|p15-18, 22, 25, 27|||Well-exposed at Mount Singleton. Includes rocks previously known as Murrouli Basalt. Lithology and geochemistry described in detail.|<2825 Ma and >2815 Ma.|Norie Group.|Quinns Basalt Member.|Is overlain by the Yaloginda Formation.||
83718|Sir Samuel Chert|70275|5|Briefly described|p477-478, 485|||Agnew-Wiluna Belt, Yilgarn Craton. Thrusting produced duplication in the Sir Samuel West and East domains; subsequently folded into anticlines. Forms a prominent ridge and a magnetic high.|||||Pyrrhotite-rich.|
22851|Sirdar Formation|61217|5|Briefly described|p21|||Comprises BIFs and mafic flows overlain by ultramafic flow and felsic flows and tuffs.In the Mount Magnet greenstone belt.||||||07-FEB-11
22851|Sirdar Formation|61853|5|Briefly described|p328|||Consists of BIF intercalated with mafic, ultramafic and felsic flows and tuffs. Geological Province: Yilgarn Craton.||||||
22851|Sirdar Formation|69744|6|Mentioned|p259|||Mount Magnet Greenstone Belt.||||||
22851|Sirdar Formation|70796|6|Mentioned|site_lithology.csv||||||||Metabanded iron formation.|
68741|Sisters Supersuite|61253|5|Briefly described| p52 Fig. 2|Archean|Archean|Comprises Radley, Portree, Indee and Langenbeck Suites. Age: 2970-2925Ma. Geological Province: Pilbara Craton.  See also p54-55 Fig. 3.||||||07-NOV-08
68741|Sisters Supersuite|63420|5|Briefly described|Map legend|Archean|Archean|Includes Wallareenya, Mallindra Well and Chillerina Granodiorites and Petermarer Monzogranite and 5 unnamed granitic units.  Includes ages: c. 2955 Ma, c. 2945 Ma and c. 2940-2930 Ma. Geological Province: Pilbara Craton.||||||15-APR-13
68741|Sisters Supersuite|63441|4|Described|p37, p10 Tb. 2|Archean|Archean|Includes four geochemically distinct suites: Indee, Langenbeck, Portree and Radley Suites. Age: 2955-2920Ma. Geological province: Pilbara Craton. Consists mainly of widespread and voluminous monzogranite. See also p31 Fig. 10, p33 Fig. 12.||||||07-FEB-11
68741|Sisters Supersuite|63538|6|Mentioned|p6 Fig. 3|Archean|Archean|Geological Province: Pilbara Craton.||||||19-APR-13
68741|Sisters Supersuite|64174|5|Briefly described|Map legend|Archean|Archean|Includes the Radley and Portree Suites. Ages for constituents: c. 2930 Ma, c. 2929 Ma, c. 2925 Ma and c. 2931 Ma.||||||15-APR-13
68741|Sisters Supersuite|64580|4|Described|map legend||Mesoarchean|Biotite monzogranite, medium to coarse grained; metamorphosed.||||||17-NOV-08
68741|Sisters Supersuite|64621|5|Briefly described|Map legend|Archean|Archean|Includes unnamed micromonzogranite dykes; local flow banding; silicified and weakly recrystallised. Occurred at the time of the North Pilbara Orogeny in c.2940Ma.||||||07-NOV-08
68741|Sisters Supersuite|64632|6|Mentioned|p203, p205|Mesoarchean|Mesoarchean||2955-2920 Ma||Includes Indee Suite.||Dominantly composed of leucocratic K-rich monzogranites.|
68741|Sisters Supersuite|64654|5|Briefly described|Map Legend|Archaean|Archaean|Includes Mulgandinnah Monzogranite. Age: c. 2928Ma and c. 2926Ma. Geological Province: Pilbara Craton.||||||17-NOV-08
68741|Sisters Supersuite|64657|5|Briefly described|Map Legend|Archaean|Archaean|Includes Coondina, Mulgandinnah and Tambourah Monzogranites. Geological Province: Pilbara Craton.||||||
68741|Sisters Supersuite|64728|6|Mentioned|p97.|||||Unit in Pilbara granite-greenstone terrane.||||
68741|Sisters Supersuite|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Pilbara Craton. Includes Woodstock, Mungarinya, Pincunah, Mulgandinnah, Keep It Dark, Eley, Coondina, Beabea, Cheearra and Abydos Monzogranites; and a mapped but unnamed unit of biotite monzogranite with K-feldspar and local quartz phenocrysts.||||||
68741|Sisters Supersuite|66118|5|Briefly described|p148 Fig.2, p153 Fig.7|||Pilbara Craton. East Pilbara Terrane.|c. 2940 Ma|||||
68741|Sisters Supersuite|66217|5|Briefly described|p1, p5, p6 Table 1, p9, p11, p42, p43.|Mesoarchean|Mesoarchean|East Pilbara Terrane, Pilbara Craton. Late tectonic granites from crustal melting intruded during the North Pilbara Orogeny.|2955-2920 Ma.|Unit in Carlindi Granitoid Complex.|Includes Indee, Langenbeck, Radley and Portree Suites.||Fine-grained granite; porphyritic biotite monzogranite.|
68741|Sisters Supersuite|67201|4|Described|p7 Fig.4, p16-17 Fig.9, see comments|||West Pilbara Superterrane. In De Grey Superbasin. Varying age ranges shown for intruding Mallina Basin: 2950-2940 Ma; 2955-2945 Ma. <3280 Ma, Nd TDM model ages (Smithies et al. 2007). Page location continued: p22-23, p57-58, p60-61, p63-64.|2955-2920 Ma||Satirist Granite, Radley Suite, Portree Suite, Indee Suite, Langenbeck Suite||Mainly leucocratic, high-K monzogranite. However 4 other compositionally distinct suites also recognized. Includes alkali granites, high-Mg diorites (sanukitoids) and monzogranites.|25-NOV-16
68741|Sisters Supersuite|68035|5|Briefly described|p291, p286 Fig 3, p290 Fig 5|Mesoarchean|Mesoarchean|NW Pilbara Craton.|2950 - 2920 Ma|||Intruded Mallina Basin units.|Alkali granites, monzogranites, and high-Mg diorites (sanukitoids); mafic-ultramafic intrusions.|
68741|Sisters Supersuite|68280|6|Mentioned|p3|Mesoarchean|Mesoarchean||2950-2920 Ma|||||
68741|Sisters Supersuite|68281|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton. Includes altered and serpentinized ultramafic rocks, with interleaved banded iron-formation and chert, collectively called the Millindinna Intrusion (not a stratigraphic name). Age of undivided constituents is c. 2940 Ma.|||Includes Petermarer Monzogranite and the informal Millindinna Intrusion.||Sheets of porphyritic monzogranite in granitic gneiss; biotite monzogranite, seriate to K-feldspar porphyritic; interleaved talc-serpentine-chlorite schist and banded iron-formation and chert; metamorphosed ultramafic rocks.|23-SEP-13
68741|Sisters Supersuite|68282|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton. 15 facies are mapped separately. Dated units range from c.2933 Ma to c.2927 Ma.|c.2930 Ma||Includes Mulgandinnah Monzogranite, Coondina Monzogranite, Eley Monzogranite, Woodstock Monzogranite.||Monzogranites, pegmatite, pegmatitic granite; generally foliated.|03-DEC-14
68741|Sisters Supersuite|68283|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|||Includes Petermarer Monzogranite, Chillerina Granodiorite, Mallindra Well Granodiorite, Wallareenya Granodiorite.|||
68741|Sisters Supersuite|69012|5|Briefly described|Map Legend|Archean|Archean|Pilbara Craton. Two unnamed facies are mapped separately.|c.2928 Ma||Includes Mulgandinnah Monzogranite and Eley Monzogranite.||Monzogranites, granodiorite, local remobilized tonalitic orthogneiss.|29-APR-14
68741|Sisters Supersuite|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton. Includes 5 unnamed sub-units mapped separately. See map legend for a detailed lithological description.|||Includes Abydos, Woodstock, Pincunah, Cheearra and Mungarinya Monzogranites and Millindinna Intrusion.|||30-APR-14
68741|Sisters Supersuite|69015|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton. Includes 3 unnamed sub-units mapped separately. See map legend for a detailed lithology.|||Includes Mulgandinnah Monzogranite, Woodstock Monzogranite, and Keep It Dark Monzogranite.||Monzogranite.|02-MAY-14
68741|Sisters Supersuite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|Sheets of grey, foliated, biotite metamonzogranite  and pegmatite dykes in tonalitic orthogneiss and leucogranite. Biotite monzogranite with K-feldspar and local quartz phenocrysts; leucocratic; massive to weakly foliated; weakly metamorphosed. Age derived from sample of hornblende-biotite metamonzodiorite (180038.1.pdf) and is the crystallization age of the monzodiorite protolith. Also includes  Beabea Monzogranite, Chillerina Granodiorite, Cheearra Monzogranite, Mallindra Well Granodiorite, Petermarer Monzogranite, Abydos Monzogranite, Eley Monzogranite, Coondina Monzogranite, Wallareenya Granodiorite.|2952 +/- 7 Ma (SHRIMP)||Includes Woodstock Monzogranite, Mulgandinnah Monzogranite, Keep It Dark Monzogranite, Mungarinya Monzogranite||Metadiorite and metagranodiorite; coarse-grained. Metagabbro, meta biotite monzogranite. K-feldspar monzogranite. Metadiorite and micromonzogranite dykes, pegmatite, metagabbro interleaved with diorite and granodiorite; metamorphosed; dolerite.|
68741|Sisters Supersuite|69185|5|Briefly described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.|||Includes Indee Suite, Langenbeck Suite, Radley Suite, Keep It Dark Monzogranite, Portree Granite, Satirist Monzogranite.|||
68741|Sisters Supersuite|69301|4|Described|p5 Fig.3, p15|||Pilbara Craton. West Pilbara Superterrane and East Pilbara Terrane.|2.95-2.94 Ga|||Intrudes Mallina Basin.|Alkali granites, monzogranites, and high-Mg diorites (sanukitoids).|
68741|Sisters Supersuite|69590|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; North Pilbara Orogeny. Sample GSWA 180038 (metamonzodiorite) yielded an interpreted igneous crystallisation age of 2952+\-7 Ma for the monzodiorite (weighted mean 207Pb/206Pb). Also includes GRANODIORITES: Chillerina, Mallindra Well, Wallareenya; Portree Granite. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.|2954-2919 Ma (inferred)||Includes Indee and Portree suites, MONZOGRANITES: Abydos, Beabea, Cheearra, Coondina, Eley, Keep It Dark, Mulgandinnah, Mungarinya, Petermarer, Pincunah, Woodstock.||Biotite monzogranite; biotite-hornblende granodiorite; dolerite; metadiorite, metagabbro and metagranodiorite; magmatically interleaved metagabbro, diorite and granodiorite; micromonzogranite dykes, pegmatite.|
68741|Sisters Supersuite|70022|6|Mentioned|p115|||West Pilbara Superterrane.||||||
68741|Sisters Supersuite|70775|4|Described|iii, p8 fig 5, p9-p10, p13|Mesoarchean|Mesoarchean|Upper Mallina Basin. Together with the Split Rock Supersuite forms the Pippingarra Granitic Complex. An age of c. 2925 Ma is given for a leucogranite in the Whim Creek Greenstone Belt. See also p15-p19, p38-p39, p41, p44 fig 27, p46, p55-p57, p60, p62, p64, p66-p67, p74-p75, p78, p81, p95.|c. 2954-2919 Ma||Includes the Radley Suite, Langenbeck Suite, Indee Suite, Portree Suite and the Radley Suite.||Leucogranite, mafic-ultramafic and felsic intrusive rocks.|
68741|Sisters Supersuite|70826|6|Mentioned|p8|Mesoarchean|Mesoarchean|East Pilbara Terrane and Karratha Terrane.||||||
68741|Sisters Supersuite|70884|6|Mentioned|p122|Mesoarchean|Mesoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|c. 3.2-2.83 Ga|||||
68741|Sisters Supersuite|71041|6|Mentioned|p42, 45 fig 2|Mesoarchean|Mesoarchean||2955-2930 Ma|||||10-NOV-17
68741|Sisters Supersuite|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||granite, monzogranite, granodiorite, felsic gneiss|
68741|Sisters Supersuite|71269|6|Mentioned|1m_geologyp12_lut.csv||||||||Undifferentiated granitoid intrusions of the Sisters Supersuite; leucogranite (locally schlieric or pegmatitic), monzogranite, granodiorite, tonalite, diorite, tonalitic orthogneiss, rhyolite dykes, pegmatite; interleaved in places|
68741|Sisters Supersuite|71550|6|Mentioned|p45|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton.|2.92-2.95 Ga|||||
68741|Sisters Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|De Grey Superbasin.  Includes Bamboo Springs, Mulgandinnah, Mungarinya, Petermarer, Beabea, Abydos, Coondina, Eley, Pilbara Creek, Pincunah, Woodstock, Satirist, Cheearra, Powdar, Keep It Dark Monzogranites, Mungaroona,Yandeearra Granodiorites, Portree Suite.|Max age 2954+/-4 Ma, min 2919+/-3 Ma.||Divided into 15 named monzogranites, 2 granodiorites and a Suite, and  and 3 unnamed units.||Granitic + ultramafic/mafic intrusive rocks. Biotite monzogranite, med./coarse grained. Both metamorphosed. Biotite monzogranite; some pheocrysts flow aligned.Phenocrystic biotite monzogranite; leucocratic. Both weakly metamorphosed; foliated.|
68741|Sisters Supersuite|72251|5|Briefly described|p54|||Geological province: East Pilbara Terrane and West Pilbara Superterrane, Pilbara Craton.||||Overlain by Split Rock Supersuite or Cutinduna Supersuite.||
68741|Sisters Supersuite|72668|5|Briefly described|p4, p9, p12, p15-17, p21, p28|||West Pilbara Superterrane. Principally developed across the Mallina Basin and western part of the EP. Geochemistry is discussed in some detail.|c. 2955-2920 Ma||Includes the Radley Suite,Portree Suite, Indee Suite and the Langenbeck Suite.||Leucocratic, high K monzogranites.|13-JAN-22
73990|Six Mile Well Ultramafic Complex|63712|5|Briefly described|p838, p839 Fig. 7|||Characterised by lens/pod accumulations of olivine accumulate - as in the Mount Keith and Perseverance Ultramafic Complexes.||||||
73849|Sixty-Six Hill Member|24391|4|Described|p8-4 Fig.2|Archean|Archean|Of Lizards Hill Formation. Black-white chert, felsic tuff and coarse quartzite with well-rounded pebble size conglomerate. Shelf facies deposit. Geological Province: Pilbara Block.||||||07-NOV-08
28155|Skates Hills Formation|22589|4|Described|p123-5,127,8,130|Cryogenian||||||||
28155|Skates Hills Formation|22816|5|Briefly described|p8 Table 1|||Of the Savory Group.||||||17-JUL-08
28155|Skates Hills Formation|22901|6|Mentioned|76 fig 2|||Geol province: Officer Basin.||||||08-SEP-08
28155|Skates Hills Formation|22907|5|Briefly described|41|||||||||
28155|Skates Hills Formation|23156|6|Mentioned|p17|||Correlated with the Loves Creek Member of the Bitter Springs Formation in the Amadeus Basin.||||||08-SEP-08
28155|Skates Hills Formation|23314|5|Briefly described|331 Fig.2|||||||||
28155|Skates Hills Formation|24161|5|Briefly described|p11|||Correlated with the Browne Formation and the Mundajini Formation.||||||
28155|Skates Hills Formation|33849|4|Described|p126|||||||||
28155|Skates Hills Formation|35596|4|Described|p9|||||||||
28155|Skates Hills Formation|36551|6|Mentioned|p101|||||||||
28155|Skates Hills Formation|37022|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
28155|Skates Hills Formation|37460|5|Briefly described|p172|||||||||
28155|Skates Hills Formation|37707|6|Mentioned|Table I|||||||||
28155|Skates Hills Formation|38243|6|Mentioned|p359|||||||||
28155|Skates Hills Formation|38898|6|Mentioned|p83|||||||||
28155|Skates Hills Formation|38988|6|Mentioned|p12|||||||||
28155|Skates Hills Formation|39168|5|Briefly described|p71|||Stromatolites||||||
28155|Skates Hills Formation|40088|6|Mentioned|p228|||||||||
28155|Skates Hills Formation|40089|2|Defined|p53|Mesoproterozoic|Mesoproterozoic|||||||
28155|Skates Hills Formation|42708|5|Briefly described|Plate 1|Proterozoic||||||||
28155|Skates Hills Formation|43229|5|Briefly described|Map Legend||Neoproterozoic|Of Savory Group.||||||28-JUL-08
28155|Skates Hills Formation|43492|3|Fully described|8|||||||||
28155|Skates Hills Formation|43756|4|Described|Fig.1,p535,537,540-1|||||||||
28155|Skates Hills Formation|44111|6|Mentioned|p.58, Fig. 2|||in Savory Basin. Includes evaporites, stromatolitic carbonates and red beds.||||||
28155|Skates Hills Formation|45149|6|Mentioned|p20|||||||||
28155|Skates Hills Formation|50188|5|Briefly described|p11 Fig. 4, p14|Neoproterozoic|Neoproterozoic|Of the Sunbeam Group. Unconformably overlies Cornelia Sandstone, Quadrio Formation. Geological Province: Officer Basin.||||||17-JUL-08
28155|Skates Hills Formation|61732|5|Briefly described|p4 Fig. 3, p58 Fig. 22|Willouran|Willouran|Of the Sunbeam Group. Geological Province: western Officer Basin.||||||07-FEB-11
28155|Skates Hills Formation|62453|3|Fully described|p5 Fig. 3, 57|Cryogenian|Cryogenian|Of the Sunbeam Group. Geological Province: Officer Basin. Dolomite, sandstone, siltstone, conglomerate. Overlies: Quadrio Formation. Lateral Correlative of Mundadjini Formation. Overlain by: McFadden Formation.||||||
28155|Skates Hills Formation|62987|5|Briefly described|p30|Neoproterozoic|Neoproterozoic|Of the Sunbeam Group. Geological Province: Officer Basin.||||||
28155|Skates Hills Formation|64283|5|Briefly described|p49, p51 Fig. 2|Neoproterozoic|Neoproterozoic|Basal unit of Sunbeam Group. Unconformably overlies Quadrio Formation. Geol.province: Officer Basin. Contains stromatolite carbonates, as well as clasts originating from either Oldham or Cornelia Sandstones. More lithology included.||||||07-FEB-11
28155|Skates Hills Formation|64286|5|Briefly described|p73 Fig. 2|||Geological Province: Officer Basin.||||||07-FEB-11
28155|Skates Hills Formation|64325|6|Mentioned|p83|||Correlative of Browne Formation.||||||28-JUL-08
28155|Skates Hills Formation|64580|4|Described|map legend||Neoproterozoic|Of Sunbeam Group. Stromatolitic dolomite, sandstone, siltstone, chert, and basal conglomerate; evaporite pseudomorphs.||||||15-DEC-08
28155|Skates Hills Formation|64772|5|Briefly described|p15, p34 Fig.22, p82, Plate 1|Neoproterozoic|Neoproterozoic|Of the Sunbeam Group. Unconformably overlain by McFadden Fm. Geological province: Officer Basin, Centralian Superbasin. Stromatolitic dolomite, sandstone, siltstone, chert and basal conglomerate; evaporite pseudomorphs.||||||25-NOV-13
28155|Skates Hills Formation|64793|6|Mentioned|p283 fig 2, p285 fig 4, p292|Cryogenian|Cryogenian|Of NW Officer Basin.||||||
28155|Skates Hills Formation|64970|6|Mentioned|p719 Fig. 2|Riphean|Riphean|Geological Province: Officer Basin.||||||27-MAY-09
28155|Skates Hills Formation|65363|6|Mentioned|p5 Fig.4, p19, p37.|Neoproterozoic|Neoproterozoic|Based on presence of Acaciella australica Stromatolite Assemblage, correlates with Browne Formation, and probably lower Mundadjini Formation. Shown as Skates Hill Fm p5 Fig. 4.||||||
28155|Skates Hills Formation|65410|6|Mentioned|p72.|Neoproterozoic|Neoproterozoic|Savory Basin.||||||
28155|Skates Hills Formation|65416|5|Briefly described|p137, pp140-141.|Neoproterozoic|Neoproterozoic|Officer Basin. Part of Sequence LP1B of Supersequence PL1. Stromatolitic dolomite has been correlated with Bitter Springs Formation (Amadeus Basin) and Woolnough Formation.|||||Thinly-bedded dolomite, chert, evaporites, fine- to medium-grained sandstone, siltstone, shale and lenticular conglomerate. Red beds at top.|
28155|Skates Hills Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|NW Officer Basin.||||||
28155|Skates Hills Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||crystalline dolostone/dolomite, chert, evaporite, sandstone|
28155|Skates Hills Formation|72034|5|Briefly described|500k_interpgeop16_lut|Tonian|Tonian|Officer Basin (Phase 1).  Age from biostratigraphy.||Sunbeam Group|||Stromatolitic dolomite, sandstone, siltstone, chert, and basal conglomerate; evaporite pseudomorphs.|
80133|Skinny Bore Granite|69583|5|Briefly described|p154|||Youanmi Terrane. Post-tectonic, low-Ca granite; typically non-reflective and appears as thin sheets in seismic profiles.||||||
76870|Skirmish Hill Formation|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. |c.1078 Ma.|Unit in Kunmarnara Group.|||Andesite and dacite, amphibole-bearing and locally amygdaloidal; rhyodacite and dacite with plagioclase phenocrysts; medium-grained granophyre, euhedral perthite and microcline crystals  surrounded by quartz and K-feldspar micrographic intergrowths.|
76870|Skirmish Hill Formation|69153|5|Briefly described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen||Kunmarnara Group|||Andesite, rhyodacite and dacite; includes layers or sheets of medium-grained granophyre|
76870|Skirmish Hill Formation|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic||1075 Ma - 1085 Ma (Inferred)|Kunmarnara Group|||Amphibole bearing and locally amygdaloidal andesite and dacite; rhyodacite and dacite. Medium grained granophyre with euhedral Perthite and microcline crystals surrounded by micrographic intergrowths of quartz and K-feldspar.|
76870|Skirmish Hill Formation|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Forms part of the basal succession of the Ngaanyatjarra Rift (Evins et al., 2010). Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 500k_interpgeop_lut.csv.|1085-1075 Ma (inferred)|Unit of Kunmarnara Group.|||Andesite and dacite; amphibole-bearing and locally amygdaloidal; layered granophyre sheets, rhyodacite.|
76870|Skirmish Hill Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||andesite, dacite, rhyodacite|
76870|Skirmish Hill Formation|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Typically metamorphosed to lowe amphibolite facies. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|1085-1075 Ma (inferred)|Unit of Kunmarnara Group.|||Andesite, rhyodacite, dacite and granophyre|
76870|Skirmish Hill Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Kunmarnara Group|||Dacitic to rhyolitic volcanic and volcaniclastic rock; minor basalt; metamorphosed.|
26900|Slatey Creek Granite|22446|6|Mentioned|p19|Statherian|Statherian|||||||
26900|Slatey Creek Granite|24197|5|Briefly described|p26, p84 Tb. 10.1|Paleoproterozoic|Paleoproterozoic|Part of the Granites Supersuite. Age: 1810Ma. Geological province: Granites-Tanami Block.||||||07-FEB-11
26900|Slatey Creek Granite|29813|4|Described|Table 2|||||||||
26900|Slatey Creek Granite|29818|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26900|Slatey Creek Granite|36532|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26900|Slatey Creek Granite|39888|6|Mentioned|Fig.7|||||||||
26900|Slatey Creek Granite|41465|6|Mentioned|p13|||||||||
26900|Slatey Creek Granite|42504|5|Briefly described|Table 3 P60|||||||||
26900|Slatey Creek Granite|45140|2|Defined|p12-13, p15-16, p22-25, p32-35, p37-38|Paleoproterozoic|Paleoproterozoic|See also p47, p74, Appx.p10. Blake et al. (1977). The Granites-Tanami Block. Scattered outcrops SW of Gardner Range; most to the S of Slatey Creek after which the unit is named. Previously mapped as part of Lewis Granite by Casey and Wells (1964). The type area is a 60m high scarp face, 16km NNW of Tent Hill, at 19deg 22'S, 128deg 41'30"E. Chemically similar to Winnecke Granophyre; geochemistry detailed.|1770 +/- 62 Ma (Rb-Sr: Page et al., 1976).|||Intrudes the Killi Killi Beds (Tanami Complex). Is overlain by Gardiner Sandstone and caps of Lewis Range Sandstone.|Porphyritic and non-porphyritic, mainly medium- to fine-grained muscovite, biotite-muscovite, and biotite adamellite; minor biotite granodiorite, pegmatite and aplite veins.|
26900|Slatey Creek Granite|46788|4|Described|p10|||Entered as in NT, but probably wrong [CEBJan97].||||||
26900|Slatey Creek Granite|46864|6|Mentioned|p37|||Re age dates||||||
26900|Slatey Creek Granite|50589|5|Briefly described|p1.4, 2.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Granites Suite/Supersuite.  Geological Province: Granites-Tanami Block.  Age: 1733 +/- 55Ma (Rb-Sr).||||||07-NOV-08
26900|Slatey Creek Granite|62580|5|Briefly described|p47|||Of the Frederick Suite. Possibly misspelt and should be MacFarlane Peak Monzogranite in the singular???||||||07-FEB-11
26900|Slatey Creek Granite|63261|6|Mentioned|p16|||Included in the Grimwade Suite.||||||07-FEB-11
26900|Slatey Creek Granite|64277|5|Briefly described|Map ledgend|Paleoproterozoic|Paleoproterozoic|Age: 1795Ma. Muscovite and biotite monzogranite; locally porphyritic; minor biotite granodiorite.||||||24-NOV-15
26900|Slatey Creek Granite|64580|4|Described|map legend||Paleoproterozoic|Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite.||||||09-DEC-08
26900|Slatey Creek Granite|64733|5|Briefly described|p170 Fig.2, p175, p176 Fig.7|Statherian|Statherian||~1795 Ma.|||Intrudes lower part of Stubbins Formation.||20-APR-12
26900|Slatey Creek Granite|66129|5|Briefly described|p213, p214, p214 Fig.1, p215 Fig.2, p217|||6000 sq. km, continuous ellipsoidal shapes. In Frederick Suite. Fine to medium grained seriate monzogranite to granodiorite, overprinted by scarce pegmatite and aplite dykes.||||||
26900|Slatey Creek Granite|66468|6|Mentioned|p16-18 Figs.2,3,5; p20, p22, p25-27|Paleoproterozoic|Paleoproterozoic|Moderately magnetic.||||||
26900|Slatey Creek Granite|67826|5|Briefly described|p401 Fig.2, p408|Statherian|Orosirian|A large pluton several tens of kilometers in diameter with a narrow (<1 km) contact hornfels zone.|~ 1793 +/- 8 Ma (Bagas et al. 2010)|||||
26900|Slatey Creek Granite|68474|6|Mentioned|p572-573|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen.||||||
26900|Slatey Creek Granite|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleoproterozoic|Paleoproterozoic|See also 100k_maginterpgeop_lut.csv, and 500k_geologyp08_lut.csv. Granites-Tanami Complex. Non- to highly magnetic. 1796 +/- 5 Ma (SHRIMP, GA).|c.1815-1790 Ma (Huston et al., in press).|Frederick Suite|||Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite.|27-NOV-15
26900|Slatey Creek Granite|69099|5|Briefly described|500k_geologyp08_lut.csv||Paleoproterozoic||||||Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite.|04-AUG-15
26900|Slatey Creek Granite|69253|6|Mentioned|p753, p757, p758|||Trans-Tanami Fault Corridor, Granites-Tanami Orogen.||||||
26900|Slatey Creek Granite|69426|6|Mentioned|p11:10|||Blake et al. (1979).||||||12-JUL-16
26900|Slatey Creek Granite|69587|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Geological province: Granites-Tanami Orogen, North Australian Craton. Events: Alice Springs Orogeny; Tanami Orogeny D1t. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|1820-1790 Ma (inferred)|||Overlain unconformably by Lewis Range Sandstone.|Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite|
26900|Slatey Creek Granite|70141|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|1820-1790 Ma.||||Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite.|
26900|Slatey Creek Granite|70142|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|1820-1790 Ma.|||Is faulted against Killi Killi Formation. Is overlain by Lewis Range Sandstone.|Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite.|
26900|Slatey Creek Granite|70143|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|1820-1790 Ma.||||Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite.|
26900|Slatey Creek Granite|70154|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic||1790-1820 Ma||||Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite|
26900|Slatey Creek Granite|71080|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. ||||Unconformably underlies Lewis Range Sandstone.||
26900|Slatey Creek Granite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Granites-Tanami Orogen. Alice Springs Orogeny (450-295 Ma); Stafford Event (1810-1790 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|1795 Ma (inferred)|Unit of The Granites Supersuite.|||Porphyritic and non-porphyritic, mainly medium to fine grained, muscovite, biotite-muscovite, and biotite monzogranite; minor biotite granodiorite. Some pegmatite and aplite veins.|
26900|Slatey Creek Granite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. Age inferred.|||||Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite.|
26900|Slatey Creek Granite|73089|6|Mentioned|p3, p8, p38|Statherian|Statherian|Geochron is an upper intercept date from Bagas et al. (2010). May be associated with the 1810-1790 Ma Stafford Event.|1793 +/- 8 Ma||||Monzogranites to granodiorites.|
81539|Sleeper Camp Formation|70802|5|Briefly described|250k_pre_mesozoic_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Madura Province. Events: Maralinga Event (1200-1100 Ma); Madura Province events (1900-1330 Ma).|1600-1100 Ma (inferred)||||Interlayered iron-rich metasedimentary rocks and metabasalt, locally with patches of quartzofeldspathic gneiss; may include intrusions of Haig Cave Supersuite and granite.|
81539|Sleeper Camp Formation|71143|5|Briefly described|p427,431,433-434,436, 440|Calymmian|Calymmian|Geological province: Madura Province. Contains variable isotopic signatures including evolved values interpreted to reflect reworking of rare slivers of hyperextended Archean crust. Includes a garnet-bearing schist with granitic veins, dated at 1538+\-17 Ma as age of crystallisation [?], and c. 1478 Ma as a metamorphic age. Assumed to be sedimentary in origin. sampled in BKD2 ~272m, at Burkin prospect.|c. 1478 Ma||||garnet-bearing schist with granitic veins|30-AUG-19
81539|Sleeper Camp Formation|73084|4|Described|p: 12, 21, 54-56, 59-60, 68-70, 74-77...|Calymmian|Calymmian|Madura Province. Lower greenschist to amphibolite grade. Shares similarities with the Malcolm Metamorphics but is slightly older and has different relationships to granitic rocks. Unit includes granitic veins, which are similar to the sodic plagiogranites of the Haig Cave Supersuite, particularly the adakite. Interpreted as subduction-related assemblages formed in an oceanic environment. Oldest known component of the oceanic arc assemblage; could mark the initiation of oceanic subduction. Denoted in the aeromagnetic data by distinctive striated banding. [Partly or wholly belongs to the Arubiddy Ophiolite Complex/complex?]. Report includes lithologic/petrographic description, structural analysis, whole-rock geochemistry, detailed geochronology, Lu-Hf. Also p: 80-82, 92-94, 111-113, 119-120, 122-124, 129-132, 137, 139, 141-142.|1536-1471 Ma||||Mafic schist (metabasalt or mafic volcaniclastic), metadolerite, schistose metasedimentary rock, cross-cutting granite and basalt or dolerite, Fe-rich, BIF-like horizons and Mn-rich layers.|
74817|Snake Gully Tonalite|64891|5|Briefly described|p37 Fig. 2, p42, p50-51 Tb. 1|Archean|Archean|Of Cullculli Suite (Annean Supersuite). Age:2751+/-6Ma. Geological province: Murchison Domain. Tonalite and quartz diorite; metamorphosed.||||||07-FEB-11
74817|Snake Gully Tonalite|69583|5|Briefly described|p49|Neoarchean|Neoarchean|Murchison Domain.||Cullculli Suite.||||
74817|Snake Gully Tonalite|69584|5|Briefly described|p5 Fig.2|Neoarchean|Neoarchean|||CullCulli Suite|||Tonalite.|
74817|Snake Gully Tonalite|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Cullculli Suite.||||
68499|Snell Well Granodiorite|63441|2|Defined|p10 Tb. 2, p36|Archean|Archean|Of the Orpheus Supersuite. Intrudes Ruth Well Formation.  Age: 3012+/-3Ma. Geological province: Pilbara Craton. Informally referred to as "Costean granodiorite" by Smith (2003).||||||07-FEB-11
68499|Snell Well Granodiorite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Orpheus Supersuite. Geological province: Pilbara Craton.  Foliated granodiorite; metamorphosed.||||||07-NOV-08
68499|Snell Well Granodiorite|64580|4|Described|map legend||Mesoarchean|Of Orpheus Supersuite. Foliated granodiorite; metamorphosed.||||||15-DEC-08
68499|Snell Well Granodiorite|67201|5|Briefly described|p16-17 Fig.9|Archean|Archean|Pilbara Craton. In Roebourne-Karratha area.||Orpheus Supersuite|||Foliated granodiorite; metamorphosed.|
68499|Snell Well Granodiorite|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Orpheus Supersuite.|||Foliated granodiorite; metamorphosed|
68499|Snell Well Granodiorite|70775|5|Briefly described|p15, p24 tbl 3|||Pilbara Craton.||Orpheus Supersuite|||Foliated granodiorite; metamorphosed.|
68499|Snell Well Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|De Grey Superbasin.|Max age 3013+/-8 Ma, 3012+/-3 Ma.|Orpheus Supersuite|||Foliated granodiorite; metamorphosed.|
77837|Snowys Dam Formation|69595|6|Mentioned|p19, p21 fig 8, p22, p23 tbl 4, |Ectasian|Ectasian|Eastern Biranup Zone or Nornalup Zone of the Arid Basin. New name for the metasedimentary component of the Fraser Range Metamorphics. Misspellt as the Snowy Dam Formation on p23 tbl 4. May have been deposited in a moderate to low-energy marine evironment. Older age is from GSWA 194778. Metamorphosed at 1304 +/- 7 Ma. See also p24 tbl 5, p24, p33, p34 fig 20, p40, p43, p44, p58.|1363 +/- 9 - 1332 +/- 21 Ma (U-Pb zircon)|||Intruded by Fraser Zone gabbro|Metasedimentary rocks intercalated with layers of mafic granulite or amphibolite. Metasedimentary rocks consist primarily of garnet-rich pelitic and semi-pelitic gneisses, with locally iron-rich rocks and quartz-rich psammitic gneiss.|
77837|Snowys Dam Formation|70090|4|Described|p441-447,449-450,452,454,460,462|Ectasian|Ectasian|Geological province: Fraser Zone, Albany-Fraser Orogen, West Australian Craton. Of Arid Basin. Intruded by granitic rocks of Recherche Supersuite and Fraser Range Metamorphics. Maximum depositional age: c. 1348 Ma. Minimum depositional age: constrained by 1304+\-7 Ma metamorphism. Paleoproterozoic detrital zircon age populations include c. 1680, 1671, 1640, 1582 and 1553 Ma. Mesoproterozoic components include c. 1497, 1466, 1455, 1444, 1401, 1382, 1366, and 1344 Ma. Contains the most dominant U-Pb detrital zircon Mesoproterozoic age component in the Barren Basin 1425-1375 Ma, subordinate components from 1475-1425 (sourced from Loogana Arc, Madura province?) and 1375-1325 Ma. Also hosts minor 1700-1650 and 1825-1725 Ma zircon age components. Hf isotope array indicates reworking of a Biranup Zone source during several melting events. ||||||
77837|Snowys Dam Formation|70153|5|Briefly described|500k_interpgeop14_lut.csv|Mesoproterozoic|Mesoproterozoic|Arid Basin, Albany-Fraser Orogen.|1334 +/- 20 Ma (isotopic) - 1305 Ma (inferred).||||Sedimentary gneiss; interlayered psammitic to pelitic, amphibolite to granulite facies gneiss; commonly interlayered with amphibolite, or mafic and felsic granulite.|
77837|Snowys Dam Formation|70182|5|Briefly described|p3, p5-6, p40-41|Mesoproterozoic|Mesoproterozoic|Arid Basin, Fraser Zone, Albany-Fraser Orogen. Affected by Stage I (1330-1260 Ma) tectonism. Anatectic melting produced syenogranitic Southern Hills Suite granites.||||Interbedded with Fraser Range Metamorphics.|Calc-silicate and iron-rich metasedimentary rocks.|
77837|Snowys Dam Formation|70732|4|Described|p285-287,291-294,297|||Geological province: Fraser Zone, Albany-Fraser Orogen. Of Arid Basin. Metamorphosed to amphibolite to granulite facies. Intruded by metamorphosed gabbroic and granitic rocks. Monazite samples yield Stage I metamorphic ages of 1285-1268 Ma (Clark et al., 2014). Monazite rims from one of those same samples yielded an age of 1234+\-17 Ma, interpreted to reflect either evidence of a second metamorphic event (Clark et al., 1999) or, alternatively, late hydrothermal growth associated with dissolution/reprecipitation reactions. LA-ICPMS titanite geochronology and SIMS zircon U-Pb geochronology presented in this study. Sample 4: LA-ICPMS metamorphic ages 1205+\-16 and 1299 +\-14 Ma; SIMS U-Pb zircon metamorphic age 1298+\-3 Ma. Youngest detrital zircon 1331+\-42 Ma. |||||Pelitic, semipelitic, and psammitic gneiss and locally calc-silicate and iron-rich metasedimentary rocks .|
77837|Snowys Dam Formation|70735|6|Mentioned|p27, 29-31, 37, 40, 42|||Arid Basin, Fraser Zone, Albany-Fraser Orogen. Foreland basin deposits. Peak granulite metamorphosed at c.1290 Ma.||||Is intruded by Fraser gabbro.|A sequence of upper amphibolite to granulite facies pelitic, semi-pelitic to calcic, locally Fe- and locally sulphide-rich metasedimentary rocks (including psammitic gneiss) with abundant layers and sills of Fraser gabbro.|
77837|Snowys Dam Formation|70802|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Fraser Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen, West Australian Craton. Metasedimentary component of the Fraser Range Metamorphics of the Fraser Zone. Events: Albany-Fraser Orogeny Stage II (1225-1140 Ma); Albany-Fraser Orogeny (1330-1140 Ma); Albany-Fraser Orogeny Stage I (1330-1260 Ma). Sample GSWA 194740 (psammitic gneiss) yielded a 207Pb*/206Pb* date of 1649+\-16 Ma, interpreted as a maximum depositional age of the sedimentary protolith; and age of high-grade metamorphism at 1283+\-8 Ma. Sample GSWA 194777 (quartzofeldspathic gneiss) yielded a weighted mean 207Pb*/206Pb* date of 1383+\-4 Ma, interpreted as maximum depositional age of the sedimentar protolith. See 500k_interpgeop14_lut.csv, 250k_pre_mesozoic_interpgeop_lut.csv.|1334+\-20 Ma; 1305 Ma (inferred)||||Sedimentary gneiss; interlayered psammitic to pelitic, amphibolite to granulite facies gneiss; commonly interlayered with amphibolite, or mafic and felsic granulite|
77837|Snowys Dam Formation|70813|5|Briefly described|p1, p5, p22-p24, p27, p39|Ectasian|Ectasian|Arid basin. Ages are interpreted as the maximum depositional and minimum depositional ages; both are derived from this publication. Peak metamorphism for this unit occurred at c. 1290 Ma and is coincident with mafic intrusions of that age.|1332 +/- 21 Ma and 1304 +/- 7 Ma||||Upper amphibolite to granulite facies, pelitic, semipelitic to calcic, locally iron- and/or sulfide rich metasedimentary rocks.|
77837|Snowys Dam Formation|70936|5|Briefly described|p58,74|Mesoproterozoic|Mesoproterozoic|Geological province: Pilbara Craton. Foreland basin deposition accompanied by magmatism and HTLP granulite facies metamorphism in the Albany-Fraser and Musgrave orogens. Protoliths to sedimentary rocks were deposited after c. 1360 Ma, prior to high-grade metamorphism and gabbro and granite intrusion starting at c. 1305 Ma (Spaggiari et al., 2014). Protoliths like derived from from an uplifted and dissected oceanic magmatic arc that was accreted to the margin by c. 1330 Ma (Spaggiari et al., 2014, 2015).||||||
77837|Snowys Dam Formation|71270|4|Described|500k_interpgeop16_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen, West Australian Craton. Of Arid Basin. Events: Albany-Fraser Orogeny Stage II (1225 - 1140 Ma); Albany-Fraser Orogeny (1330 - 1140 Ma); Albany-Fraser Orogeny Stage I (1330 - 1260 Ma).|1332+\-21 Ma; 1304+\-7 Ma||||Sedimentary gneiss; psammitic, semipelitic, and locally calc-silicate and iron-rich layers; commonly interlayered with metagabbro, or mafic and felsic granulite|
77837|Snowys Dam Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Arid Basin.|Max age 1332+/-21 Ma, min 1304+/-7 Ma.||||Sedimentary gneiss; psammitic, semipelitic, and locally calc-silicate and iron-rich layers; commonly interlayered with metagabbro, or mafic and felsic granulite. Interlayered psammitic and pelitic gneiss, gabbroic gneiss, and felsic granulite.|
77837|Snowys Dam Formation|72059|5|Briefly described|p57,67|Ectasian|Ectasian|Geological province: Fraser Zone, Albany-Fraser Orogen. Of Arid Basin. Deposited on the accretion portion of the Madura Province after 1332+\-21 Ma (age of youngest detrital zircon) and before 1304+\-7 Ma (age of metamorphic zircon growth) (Spaggiari et al., 2015). Comprises upper amphibolite to granulite facies metasedimentary rocks dominated by sulphide- and/or iron-rich metapelitic and metasemipelitic rocks (Spaggiari, 2014a, 2015). Contains c. 1410 Ma Loongana Arc zircon detritus that is distinct in both its age and isotopic composition to anything else within the region. Interpreted to have been deposited proximal to a subduction zone system c. 1450-1360 Ma to aloow the outboard Loongana Arc to be obducted and eroded.|1332 +/- 21 Ma (Spaggiari et al, 2015)|||||03-FEB-20
77837|Snowys Dam Formation|72710|6|Mentioned|p2, p4 Fig.2, p17, 20.|Mesoproterozoic|Mesoproterozoic|Shown as part of Arid basin (1600 to 1310 Ma). Said to have contributed sulphur to magmatic sulfide deposits of the Fraser Zone.|1600 Ma to 1310 Ma.||||Includes metasedimentary rocks.|
77837|Snowys Dam Formation|73084|6|Mentioned|p12, p56, p139-141|||Arid Basin. Albany-Fraser Orogen, Kepa Kurl Booya Province, Fraser Zone. Possibly deposited in a developing foreland basin setting including detritus from both the continental margin and oceanic arc.||||||
77837|Snowys Dam Formation|73480|6|Mentioned|p217|||Arid Basin.||||||
77837|Snowys Dam Formation|73597|5|Briefly described|p1177, 1179, 1182, 1185, 1187-1193|||Fraser Zone, Albany-Fraser Orogen. Hosts the Fraser Gabbro suite of intrusions including the 1304 +/- 22 Ma Nova-Bollinger Ni-Cu-Co deposit; part of voluminous mafic-ultramafic intrusions into these uppermost Arid Basin sediments. Nd and Sr isotope data tabulated. S isotopes histograms, graphs; discussion.|||||Gneisses, calc-silicates, marbles, granulites: metamorphosed pelitic and psammitic sediments, marls, limestones, iron-formations and probable volcaniclastic rocks. Includes a voluminous suite of mafic-ultramafic intrusions.|
70124|Soanesville Group|63441|2|Defined|p4 Tb. 1, p21|Archean|Archean|Of Pilbara Sup'group.Supersedes Soanesville Subgp (Gorge Ck Gp). Comprises Cardinal, Corboy, Paddy Market and Pyramid Hill Fms and Honeyeater Basalt. Disconform.on Sulphur Springs Gp; unconform.below De Grey Supergp. Max.thick: 6000m. East Pilbara Terrane||||||07-FEB-11
70124|Soanesville Group|63538|4|Described|p2 Fig. 1, p3 Fig. 2, p5, p10, p16|Archean|Archean|Of Pilbara Supergroup. Includes five units. Overlain disconformably by Gorge Creek Group. Underlain by Sulphur Springs Group. Geological Province: Pilbara Craton. Banded iron-formation, sandstone and shale.||||||19-APR-13
70124|Soanesville Group|64405|5|Briefly described|p2 Fig. 1, , p4 Fig. 3|Archean|Archean|Of the Pilbara Supergroup. Geological province: East Pilbara Terrane.||||||07-FEB-11
70124|Soanesville Group|64632|6|Mentioned|p201 Fig.1, p202|Mesoarchean|Paleoarchean|East Pilbara terrane.|3235-3165 Ma|Of the Pilbara Supergroup.||Overlies Sulphur Springs Group|Dominantly sedimentary rocks.|
70124|Soanesville Group|65757|5|Briefly described|p83 Fig.3, p85|||Coppin Gap region, arenites, unconformably overlies the Sulphur Springs Group.||||||
70124|Soanesville Group|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Pilbara Craton. Includes Cardinal, Corboy, Paddy Market and Pyramid Hill Formations and Honeyeater Basalt.||||||
70124|Soanesville Group|66118|4|Described|p146-149, p151, p154-155, p157-159|||Pilbara Craton. East Pilbara Terrane. Max Thickness: 4300 m in type area (Soanesville Syncline); 3500m (lower siliciclastic succession). Age: c. 3190 Ma, U-Pb xenotime, minimum age of deposition (Rasmussen et al. 2007). Intrusive Dalton Suite age (3182+/-2 Ma SHRIMP U-Pb zircon) interpreted as igneous emplacement age of sill as well as eruptive age of associated Honeyeater Basalt (Soanesville Group). Shown as Soanesville group on p148.|c. 3200-3180 Ma. See comments.|Stratigraphically highest in Pilbara Supergroup|Honeyeater Basalt|Disconformably to unconformably overlies Sulphur Springs Group (onlapping lower disconformable contact). Is intruded by subvolcanic sills of Dalton Suite.|Includes lower siliciclastic (sandstone, silstone, shale, gravelly turbiditic units) succession (>1600 m, up to 3500m thick), which is conformably overlain by basalt (1000-2000m thick) and intruded by associated subvolcanic sills.|26-MAY-20
70124|Soanesville Group|66122|6|Mentioned|p74|Archean|Archean||c.3.19 Ga.|Pilbara Supergroup.||||
70124|Soanesville Group|66217|5|Briefly described|p6 Table 1, p10, p14, p38.|Mesoarchean|Mesoarchean|Deposition during rifting of East Pilbara Terrane margins and basin formation within the East Pilbara Terrane at 3200-3165 Ma. Tilted by Prinsep Orogeny 3070-3050 Ma.|3200-3165 Ma.|||Unconformably overlies Pilbara Supergroup.|Low-grade metasedimentary and metavolcanic rocks.|
70124|Soanesville Group|66664|6|Mentioned|p3.  |||Fortescue Basin.||||||
70124|Soanesville Group|66745|3|Fully described|pp52-55.|Mesoarchean|Mesoarchean|Western part of East Pilbara Terrane. Represents earliest stage of a Mesoarchean Wilson cycle, rifting the Pilbara Craton. Now excluded from Pilbara Supergroup because its deposition marked a major change in tectonic processes operating in the craton.|c.3200-3190 Ma.|Formerly of the Pilbara Supergroup.|Includes Cardinal, Corboy, Paddy Market and Pyramid Hill Formations, Honeyeater Basalt, and Budjan Creek Formation.|Overlies Sulphur Springs Group.|A >2500 m thick succession of siliciclastic sedimentary rocks containing minor chert and BIF, overlain by volcanic rocks.|12-OCT-15
70124|Soanesville Group|67130|5|Briefly described|p16|Mesoarchean|Paleoarchean||3230 -3170 Ma||Includes Cardinal Formation, Corboy Sandstone, Paddy Market Formation, Honeyeater Basalt, Pyramid Hill Formation,|Conformably (or disconformably) overlies Sulphur Springs Group|Clastic sedimentary rocks, basalt and banded iron formation.|
70124|Soanesville Group|67197|5|Briefly described|p2-5|Paleoarchean|Paleoarchean|See Hickman et al. (in prep.). Originally defined (Lipple, 1975) as a Subgroup within the Gorge Creek Group. East Strelley greenstone belt.|3190-3180 Ma.||Cardinal, Corboy, Paddy Market, Pyramid Hill Formations; Honeyeater Basalt.|Unconformably overlies Pilbara Supergroup. Is overlain unconformably by Gorge Creek Group.||
70124|Soanesville Group|67201|4|Described|p7 Fig.4, p12 Tb.1, p14, p20, p26|||In northern Pilbara Craton, East Pilbara Terrane, Soanesville Basin, rift-related successions.Tectonic contact (Regal Thrust) at top.|c. 3190 - 3180 Ma||Pyramid Hill Formation, Honeyeater Basalt, Paddy Market Formation, Corboy Formation, Cardinal Formation|Suggested as analogue of Ruth Well Formation. Is overlain by Gorge Creek Group, with angular unconformity.||25-NOV-16
70124|Soanesville Group|67269|6|Mentioned|p5|Paleoarchean|Paleoarchean||||Honeyeater Basalt, Corboy Formation.|||
70124|Soanesville Group|67270|6|Mentioned|p3|Paleoarchean|Paleoarchean|Rift-related succession.||||||
70124|Soanesville Group|67668|6|Mentioned|Fig. 2; p. 154||Mesoarchean|East Pilbara Terrane, Pilbara Craton.|3200 - 3165 Ma.|Pilbara Supergroup|Cardinal, Corboy, Pyramid Hill and Paddy Market Formations, and Honeyeater Basalt.|Overlies the Sulphur Springs Group, underlies the De Grey Supergroup (Gorge Creek Group) unconformably.|Mostly clastic sedimentary sequence with minor basalt (commonly pillowed) and banded iron formation.|
70124|Soanesville Group|68035|5|Briefly described|p289, 293, p286 Fig 3|Mesoarchean|Paleoarchean|Soansville Basin. On NW margin of East Pilbara Terrane.?shallow-water clastic successions and thick volcanic piles, in passive margin settings. May include microbial mats.|3220 - 3190 Ma|||||
70124|Soanesville Group|68280|6|Mentioned|p3, p19 fig 16|Mesoarchean|Paleoarchean||3220-3190 Ma|||||17-JAN-23
70124|Soanesville Group|68282|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|< 3220 Ma||Includes the Paddy Market Formation, Corboy Formation, Cardinal Formation.|||
70124|Soanesville Group|68284|5|Briefly described|p4, 7|||Crops out in the Marble Bar-Nullagine area, East Pilbara Terrane. Microbial mats and microfossils have been reported from the lower part of this Group.|3220-3165 Ma.|||Locally, unconformably overlies Kelly Group.||
70124|Soanesville Group|69012|5|Briefly described|Map Legend|Archean|Archean|Soanesville Basin.|||Includes the Budjan Creek Formation.|||
70124|Soanesville Group|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Soanesville Basin.|||Includes Honeyeater Basalt, Paddy Market Formation, and Corboy Formation.|||30-APR-14
70124|Soanesville Group|69015|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|||Includes Honeyeater Basalt; Pyramid Hill, Paddy Market, Corboy and Cardinal Formations.|||02-MAY-14
70124|Soanesville Group|69167|6|Mentioned|geologyp_lut.csv|Mesoarchean|Mesoarchean|Intruded by unnamed gabbro sill that is dated at 3185 +/- 2 Ma. ||Soanesville Group|Includes Honeyeater Basalt, Cardinal Formation|||
70124|Soanesville Group|69301|4|Described|p5 Fig.3, p9 Tb.1, p12-14, p20-22|||Pilbara Craton. East Pilbara Terrane. Soanesville Basin. Rift-related successions. Min. depositional age: 3.19 Ga based on a U-Pb data from monazite and xenotime (Rasmussen et al. 2007). Submarine environments ranging from mid-fan to outer-fan and basin-plain.|3200-3170 Ma. See comments.||Pyramid Hill Formation, Honeyeater Basalt, Paddy Market Formation, Corboy Formation, Pilbara Well volcanics (informal), Cardinal Formation|Intruded by Dalton Suite. Overlies Budjan Creek Formation. Unconformably overlies Sulphur Springs Group. Is unconformably (angular) overlain by Gorge Creek Group.||
70124|Soanesville Group|69563|6|Mentioned|p690 Tb.1|||Pilbara Craton. Contains an olistostrome, overlain by arenite, felsic tuff and BIF.||||||
70124|Soanesville Group|69590|5|Briefly described|GEOL_LUT_CSV files + geochron files|||Geological province: Pilbara Craton. Of Soanesville Basin. Metamorphosed tyo upper greenschist to amphibolite facies. Sample GSWA (rhyolitic volcaniclastic rock) yielded an interpreted maximum depositional age of 3180+\-6 Ma for the volcaniclastic rock (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|||Includes Budjan Creek Formation, Cardinal Formation, Corboy Formation, Honeyeater Basalt, Paddy Market Formation, Pyramid Hill Formation.|Overlain by Kangaroo Caves Formation.||
70124|Soanesville Group|69616|5|Briefly described|p159-165, p169, p180-183|||Has syndepositional structures: slump folds and bedding-parallel pinch and swell structures. Age range inferred from surrounding units.|c.3228-c.3020 Ma.||Includes Cardinal, Corboy, Paddy Market and Pyramid Hill Formations and Honeyeater Basalt.|Overlies Kangaroo Caves Formation.|Turbiditic sedimentary and volcanic rocks.|
70124|Soanesville Group|70022|5|Briefly described|p113-116|||Soanesville Basin, East Pilbara Terrane. Up to 3.5 km thick. Associated with a rifting episode.|3220-3165 Ma.||Budjan Creek, Corboy, Paddy Market, Pyramid Hill Formations; Honeyeater Basalt.|Unconformably overlies Sulphur Springs Group. Is overlain unconformably by Gorge Creek Group.|Clastic succession, including feldspathic sandstone and metasandstone, and volcaniclastic metasandstone.|
70124|Soanesville Group|70729|6|Mentioned|p164|||Geological province: East Pilbara Terrane, Pilbara Craton.||||||
70124|Soanesville Group|70733|6|Mentioned|p105 Fig.1|||Eastern Pilbara Craton.||||||
70124|Soanesville Group|70775|5|Briefly described|p12, p29, p47, p68, p99-p100|Paleoarchean||East Pilbara.|<3220 Ma||Includes the Cardinal Formation, Corboy Formation, Paddy Market Formation and the Honeyeater Basalt.|Unconformably overlies the Sulphur Springs Group. Faulted against the Regal Formation.||
70124|Soanesville Group|70826|6|Mentioned|p6 tbl 2, p8|Mesoarchean|Mesoarchean|Soanesville Basin, east Pilbara Terrane. ||||Is intruded by the Mount Billroth Supersuite.||
70124|Soanesville Group|70884|5|Briefly described|p122,135|Mesoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|3.53-3.18 Ga||Includes Budjan Creek Formation.|||
70124|Soanesville Group|71041|5|Briefly described|p45 fig 2||||3190 Ma|Shown as of Pilbara Supergroup.|Includes the Corboy Formation, Honeyeater Basalt.|Overlies the Sulphur Springs Group. Overlain by the Gorge Creek Group.||07-NOV-17
70124|Soanesville Group|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||conglomerate, sandstone, greywacke, banded iron formation, komatiitic (high-Mg) basalt, ultramafic schist|
70124|Soanesville Group|71487|5|Briefly described|p128|Archean|Archean|Of De Grey Superbasin.||||Overlain by De Grey Supergroup. Underlain by Pilbara Supergroup.||
70124|Soanesville Group|72034|6|Mentioned|500k_interpgeop16_lut|Mesoarchean|Paleoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Pyramid Hill Formation.|||
70124|Soanesville Group|72251|5|Briefly described|p52,54|Mesoarchean|Mesoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Deposited during separation of Karratha Terrane from the East Pilbara Terrane c. 3.2 Ga.|3220-3165 Ma||Includes Pyramide Hill Formation, Honeyeater Basalt, Paddy Market Formation, Corboy Formation and Budjan Creek Formation.|Overlain unconformably by Gorge Creek Group. Underlain unconformably by Sulphur Springs Group.||
70124|Soanesville Group|72668|4|Described|p3, p4, p5-6, p19, p28|||East Pilbara Terrane. Reaches a maximum thickness of c. 2600m. Thick deep water sedimentary basin fill. Inferred to have been deposited soon after Sulphur Springs Group ~3230-3170 Ma.||Pilbara Supergroup|Includes the Cardinal Formation,  ?Pincunah Hill Formation,Corboy Formation, Paddy Market Formation, Honeyeater Basalt and the Pyramid Hill Formation.|Disconformably overlies the Sulphur Springs Group.|Clastic sedimentary rocks, basalt and banded-iron formation.|13-JAN-22
70124|Soanesville Group|73598|6|Mentioned|p1212|Mesoarchean|Paleoarchean|East Pilbara Terrane.|||Budjan Creek, Corboy, Paddy Market, Pyramid Hill Formations; Honeyeater Basalt.|Unconformably overlies Sulphur Springs Group. Is overlain unconformably by Gorge Creek Group.||
77938|Songvang Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||2820 - 2711 Ma (inferred).||||Foliated, fine-grained metamorphosed mafic rock. Basalt; fine grained with local pyroxene spinifex textures, minor interflow sedimentary rocks. Komatiite; fine grained with local olivine spinifex texture; metamorphosed.|
77938|Songvang Formation|71212|5|Briefly described|intro p2, intro p3|||Yilgarn Craton. ||||Overlies the Donegal Komatiite, Fourteen Mile Well Foramtion or the Satellite Igneous Complex. Overlain by the Knobbly Gabbro.||
77938|Songvang Formation|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2820-2711 Ma (inferred)||||Basalt; fine grained with local pyroxene-spinifex texture; includes medium-grained layers and lenses; minor interflow sedimentary rocks; metamorphosed; komatiite with local olivine-spinifex texture; foliated fine-grained metasedimentary mafic rock.|
77938|Songvang Formation|73151|5|Briefly described|p3|Neoarchean|Neoarchean|Yilgarn Craton. Kalgoorlie Terrane, Agnew Greenstone Belt.||Kalgoorlie Group||Overlies Fourteen Mile Well Formation, underlies Never Can Tell Basalt.|Basalt.|
27569|Sophie Downs Granite|22764|4|Described|Table1,p7||Paleoproterozoic|Uncomformable beneath Mount Parker Sandstone||||||01-FEB-10
27569|Sophie Downs Granite|23621|5|Briefly described|p14|||Replaced with Sophie Downs Granophyre Member.||||||
27569|Sophie Downs Granite|24173|5|Briefly described|p7, 15|Paleoproterozoic|Paleoproterozoic|Geological Province: Halls Creek Orogen. Superseded by Sophie Downs Granophyre Member.||||||07-NOV-08
27569|Sophie Downs Granite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Age: 1910Ma. Geological province: Kimberley Province. (Of the Sophie Downs Suite or Supersuite??)||||||07-FEB-11
27569|Sophie Downs Granite|29845|6|Mentioned|p120|||||||||
27569|Sophie Downs Granite|30892|6|Mentioned|p97|||Ca. 2100m.y.||||||
27569|Sophie Downs Granite|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27569|Sophie Downs Granite|31393|6|Mentioned|Pl.25|||||||||
27569|Sophie Downs Granite|32728|6|Mentioned|Fig.3|||||||||
27569|Sophie Downs Granite|33443|6|Mentioned|p260|||||||||
27569|Sophie Downs Granite|35120|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27569|Sophie Downs Granite|36885|4|Described|p175|||||||||
27569|Sophie Downs Granite|37462|6|Mentioned|Fig.4.6|||||||||
27569|Sophie Downs Granite|37633|4|Described|Table 65|||See also P97.||||||
27569|Sophie Downs Granite|41465|5|Briefly described|p9|||||||||
27569|Sophie Downs Granite|41977|4|Described|p471|||||||||
27569|Sophie Downs Granite|42326|5|Briefly described|Fig.11 P9|||||||||
27569|Sophie Downs Granite|42768|6|Mentioned|Fig.6|||||||||
27569|Sophie Downs Granite|44155|4|Described|p242 Tb.3-5, p243 Tb.3-6, p248 Tb.3-8|||East Kimberley. Late to post-tectonic faulting: 1815 +/- 14 Ma.||Lamboo Complex||Intrudes Whitewater Volcanics, Halls Creek Group.|Medium-grained granite or granophyric granite; some microgranite.|
27569|Sophie Downs Granite|44324|14|Not recorded|p.7||Proterozoic|Tb.1, (Proterozoic). See page 16, 17.||||||
27569|Sophie Downs Granite|44325|14|Not recorded|map legend||Proterozoic|Proterozoic.||||||
27569|Sophie Downs Granite|44397|14|Not recorded|p.8, Table 1||Proterozoic|Lamboo Complex.||||||
27569|Sophie Downs Granite|44398|14|Not recorded|map legend||Proterozoic|||||||
27569|Sophie Downs Granite|45047|4|Described|p13|||See p25. Lamboo Complex.||||||19-MAY-15
27569|Sophie Downs Granite|45048|3|Fully described|p63|||See also p64-65.||||||19-MAY-15
27569|Sophie Downs Granite|46797|6|Mentioned|p81|||Dates||||||
27569|Sophie Downs Granite|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Sophie Downs Suite. Age: 1912 +/- 5Ma (Shrimp). Underlies: Saunders Creek Formation (unconformably).||||||07-NOV-08
27569|Sophie Downs Granite|60724|4|Described|p6, p5 Fig. 2|Paleoproterozoic|Paleoproterozoic|Within the Lamboo Complex. Fine grained, partially recrystallised muscovite-biotite feldspar granite, with a microgranitic or granophyric texture. Unconformably overlain by Saunders Creek Formation. Age: 1.92-1.90Ga. ||||||07-NOV-08
27569|Sophie Downs Granite|64104|6|Mentioned|p76 fig 10|Paleoproterozoic|Paleoproterozoic|||||||
27569|Sophie Downs Granite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Data from OZCHRON1. Abbrev. comment: The data give a very reliable age, close to the age of the Ding Dong Downs Volcanics.' ?Previously called Sophie Downs Granophyre Member of Ding Dong Downs Volcanics?|Crystallisation age: 1912+/-5 Ma U/Pb SHRIMP|Sophie Downs Suite||Similar age to Ding Dong Downs Volcanics.|Variably foliated leucocratic and granophyric metamonzogranite.|04-AUG-15
27569|Sophie Downs Granite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv. |1912-2435 Ma|Sophie Downs Suite|||Variably foliated leucocratic and granophyric metamonzogranite.|
27569|Sophie Downs Granite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2.|1912-1912 Ma (Isotopic)|Unit of Sophie Downs Suite.|||Variably foliated leucocratic and granophyric metamonzogranite|
27569|Sophie Downs Granite|70154|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv.|1912 Ma||||Variably foliated leucocratic and granophyric metamonzogranite.|
27569|Sophie Downs Granite|71267|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See also geochron files.|1912+\-4 Ma (isotopic)|Unit of Sophie Downs Suite.|||Variably foliated leucocratic and granophyric metamonzogranite|
27569|Sophie Downs Granite|71397|4|Described|p4,8,10,12,27,30-32,36,40|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen. Blake et al. (1999b) dated a leucocratic monzogranite from the Sophie Downs Dome at 1912+\-3 Ma (GA 87598029). See p19 for detailed major and trace-element geochemical analysis. Sm-Nd whole-rock isotope analysis showed an evolved Nd mantle signature (ENd=-3.82; GSWA 108550), with a TDM2 model age for a c. 2600 Ma mantle source. Zircon U-Pb geochronological analysis of sample GA 87598029 (foliated porphyritic granophyre) yielded a weighted mean 207Pb*/206Pb* date of 1912+\-4 Ma, interpreted as the age of magmatic crystallisation.|1912+\-3 Ma|Unit of Sophie Downs Suite.||Overlain unconformably by Brim Rockhole Formation.||28-NOV-19
27569|Sophie Downs Granite|72437|5|Briefly described|p7, p51|Palaeoproterozoic|Palaeoproterozoic|Together with the Ding Dong Downs Volcanics forms basement to the Halls Creek Group.|c. 1910 Ma|Sophie Downs suite|||Recrystallised fine-grained monzogranite.|
41468|Sophie Downs Suite|50437|5|Briefly described|p1.6, 5.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Age: 1910Ma. Geological Province: Kimberley Region.||||||07-NOV-08
41468|Sophie Downs Suite|61861|6|Mentioned|Fig.2.||||1912 Ma.||||Granites.|
41468|Sophie Downs Suite|68078|6|Mentioned|p7 figure 4|Paleoproterozoic|Paleoproterozoic||~1910 Ma|||||
41468|Sophie Downs Suite|69003|5|Briefly described|p5, p19|Paleoproterozoic|Paleoproterozoic|E zone, Lamboo Province, Halls Creek Orogen. Coeval with Ding Dong Downs Volcanics.|c.1910 Ma.|||Is overlain by Halls Creek Group.|Granitic rocks.|
41468|Sophie Downs Suite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.|||Includes Esaw Monzogranite, Junda Microgranite, Sophie Downs Granite, Ding Dong Downs Volcanics.||Leucocratic metagranite, metarhyolite, metabasalt and amphibolite, and minor metasedimentary rock.|04-AUG-15
41468|Sophie Downs Suite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv.|||Includes Sophie Downs Granite, Ding Dong Downs Volcanics||Leucocratic metagranite, metarhyolite, metabasalt and amphibolite, minor metasedimentary rock.|
41468|Sophie Downs Suite|69585|6|Mentioned|p4|Orosirian|Orosirian|Eastern Lamboo Province.||||||
41468|Sophie Downs Suite|69597|6|Mentioned|p5 fig 2b|||||||||
41468|Sophie Downs Suite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2. See 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|1913-1907 Ma (Isotopic)||Includes Ding Dong Downs Volcanics, Esaw Monzogranite, Junda Microgranite, Sophie Downs Granite.||Leucocratic metagranite, metarhyolite, metabasalt and amphibolite, and minor metasedimentary rock|
41468|Sophie Downs Suite|70154|6|Mentioned|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv.|1907-1913 Ma||Ding Dong Downs Volcanics|||
41468|Sophie Downs Suite|70731|6|Mentioned|p268|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.||||||
41468|Sophie Downs Suite|70812|5|Briefly described|p6, p27, p29|Orosirian|Orosirian|Central Zone of the Halls Creek Orogen, Lamboo Province.|c. 1900 Ma|||||
41468|Sophie Downs Suite|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|||||||
41468|Sophie Downs Suite|70851|4|Described|p3-p4, p19, p28|Paleoproterozoic|Paleoproterozoic|Eastern Zone, Lamboo Province.|c. 1910 Ma||Includes the Ding Dong Downs Volcanics.|Unconformably overlain by the Halls Creek Group.||
41468|Sophie Downs Suite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv and geochron files.|1913+\-5 to 1907+\-6 Ma (isotopic)||Includes Sophie Downs Granite, Ding Dong Downs Volcanics, Esaw Monzogranite, Junda Microgranite.|Overlain by Halls Creek Group.||
41468|Sophie Downs Suite|71397|3|Fully described|p1-8,14,19,30-31,42-43,45,47-48|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen. Oldest exposed rocks in the Eastern Zone, Lamboo Province. Records passive margin magmatism and sedimentation between c. 1912 and 1904 Ma. Forms restricted inliers in the widespread volcano-sedimentary sequences of the Halls Creek Group. Metafelsic rocks of the Sophie Downs Suite have A-type granite geochemical signatures and are metaluminous to peraluminous; it may represent passive margin volcanism, magmatism and crustal assimilation on the North Australian Craton. See p19 for detailed major and trace-element geochemical analysis. Radiogenic zircon EHf values from the Sophie Downs Suite suggest mantle contribution during passive margin magmatism along the western margin of the North Australian Craton. Sm-Nd whole-rock data of felsic and mafic rocks in the Sophie Downs Suite indicate mixing of juvenile mafic magma with sediment or older crust to produce near CHUR ENd values.|1912-1904 Ma||Includes Sophie Downs Granite, Junda Microgranite, Esaw Monzogranite, Ding Dong Downs Volcanics.|Overlain unconformably by Halls Creek Group. Intruded by Woodward Dolerite.|Greenschist facies granitic rocks, bimodal volcanic and metasedimentary rocks.|
41468|Sophie Downs Suite|71873|5|Briefly described|p427,434|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province. Oldest exposed rocks in the Eastern Zone. Records passive margin magmatism and sedimentation between c.  1912 and 1904 Ma (Phillips et al., 2016; Sheppard et al., 1999) in the Eastern Zone. Intruded by Woodward Dolerite during Halls Creek Orogeny c. 1832-1808 Ma.|||Includes Ding Dong Downs Volcanics.|Overlain unconformably by Halls Creek Group.||
41468|Sophie Downs Suite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Halls Creek Orogen.|Max age 1913+/5 Ma, 1907+/-6 Ma.||||Leucocratic metagranite, metarhyolite, metabasalt and amphibolite, and minor metasedimentary rock.|
41468|Sophie Downs Suite|72377|5|Briefly described|p8,14,16|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Possible source for c. 2400 Ma to c. 1900 Ma detrital zircons reported in McArthur Basin.|c. 1904 Ma|||||
41468|Sophie Downs Suite|73089|6|Mentioned|p26, p28|||Basement to the Halls Creek Group.||||Unconformably overlain by Saunders Creek Formation (Halls Creek Group).||
41468|Sophie Downs Suite|73158|6|Mentioned|p10|||Halls Creek Orogen. Eastern Zone.|||Ding Dong Downs volcanics|||
41468|Sophie Downs Suite|73159|5|Briefly described|p10|||Oldest rocks in the Halls Creek Orogen (Eastern Zone).|||Ding Dong Downs volcanics.||Includes mafic volcanic and sedimentary rocks.|
41468|Sophie Downs Suite|73427|6|Mentioned|p2|Orosirian|Orosirian|North Australian Craton, Lamboo Province.|ca. 1910 Ma|||||
23980|Sorby Dolomite Member|13194|4|Described|p391 Tb. 4-16|||Type Section: Elf Aquitaine drill hole WBS 5048 15o27'S 128o59'E (199-280.4m).  Correlated to bottom 122m of type section of Burt Range Formation.||Burt Range Formation, at Sorby Hills||Overlies Buttons Formation (local unconformably). Overlain by Knox Siltstone Member (locally disconformably).|Dolomite, dolomitic siltstone, and silty shale.|
23980|Sorby Dolomite Member|40792|2|Defined|p177|early Tournaisian|early Tournaisian|Mention P177 as Sorby Dolomite||||||
23980|Sorby Dolomite Member|41864|5|Briefly described|p102|||||||||
23980|Sorby Dolomite Member|42175|5|Briefly described|p197|||See also Fig.2||||||
23980|Sorby Dolomite Member|45169|6|Mentioned|Fig.4|||||||||
23980|Sorby Dolomite Member|64694|5|Briefly described|p235, p239, p252-253, p254 Fig.12|Tournaisian|Tournaisian|||Unit in Burt Range Formation.||Is unconformably overlain by Knox Siltstone Member.||
34477|South Caroline Clay|22769|3|Fully described|p764-65,Table3p764|Pliocene|Miocene|Top unit of Salt River Group. Clays ranging from ferruginous greyish clay to gravelly green clay with slight brown striations; lenses formed in some areas - greenish sand, medium to coarse, subrounded to rounded. Thickness: 6m. Overlies the Yenyening Fm.||||||17-JAN-06
34477|South Caroline Clay|65194|5|Briefly described|p124 Fig.4.30, p125|||Unit in Salt River Group. Relatively uniform consisting of grey, whitish grey, and green clay and silt. It is undated but overlies the Miocene Yenyening Formation.||||||
70136|South Mallina Basalt Member|63441|2|Defined|p5 Tb.1, p29|Archean|Archean|Of Bookingarra Formation (Croydon Group, Pilbara Supergroup). Geological province: Mallina Basin, Pilbara Craton.||||||07-FEB-11
70136|South Mallina Basalt Member|63538|4|Described|p32, p33, p34, p35|Archean|Archean|Of Bookingarra Formation. Geological Province: Pilbara Craton. Subaqueous flows and hyaloclastite deposits of high-Si basalt.||||||07-FEB-11
70136|South Mallina Basalt Member|67201|5|Briefly described|p21 Fig.12, p58-61, p63|||In northwestern Pilbara Craton, West Pilbara Superterrane and East Pilbara Terrane, De Grey Superbasin, Mallina Basin. Shown as South Mallina Basalts on some figures.||Bookingarra Formation|||Siliceous high-Mg basalt flows.|
70136|South Mallina Basalt Member|69590|4|Described|250k_interpgeop_lut.csv|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton. Of Mallina Basin, De Grey Superbasin. Events: North Pilbara Orogeny.|2964-2943 Ma (inferred)|Unit of Croydon Group.|||Siliceous high-Mg basalt; typically variolitic, commonly pyroxene spinifex-textured, and pillowed|
70136|South Mallina Basalt Member|70775|5|Briefly described|p29 tbl 5, p56, p59|Mesoarchean|Mesoarchean|Mallina Basin.|c. 2950 Ma (Smithies et al 2004a)|||||
70136|South Mallina Basalt Member|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mallina Basin.||Bookingarra Formation|||Siliceous high-Mg basalt; typically variolitic, commonly with pyroxene spinifex textures, and pillowed.|
70136|South Mallina Basalt Member|72668|6|Mentioned|p15||||||||Silicic, high-Mg basalt.|14-JAN-22
80798|South Perth Sequence 1|71958|4|Described|p48, p51, p54, p62, p64-p65, p67, p79|Valanginian|Valanginian|Vlaming Sub-basin. This unit is named for the South Perth Shale. A type locality is only described as "offshore, not penetrated by any wells."  Lithology is unknown but "thought to contain siliciclastics and some volcanics and volcaniclastics." On the basis of 2D seismic work is thought to be approximately 340m thick. Interpreted to have been deposited in a fluvio-deltaic to deep marine environment.||South Perth Supersequence||Conformably overlain by South Perth Sequence 2.||
80799|South Perth Sequence 2|71958|2|Defined|p51, p54-p56, p62|Hauterivian|Valanginian|Vlaming Sub-basin. This unit is named for the South Perth Shale. This sequence comrpises the Gage Sandstone, South Perth Shale and in places, the Leederville Formation. The type locality occurs in Charlotte 1 (-31.808795, 115.450375) in the interval between 1574.4 and 766 m (total thickness of 808.4m). Thickness in wells ranges from 0 to 827.1m (Mullaloo 1) and is penetrated by all wells in the study area except for Roe 1. Age determined by the presence of diagnostic microsfossils including G. mutabilis, K. scrutillinum, P. lowryi and A. alata Dinocyst zones. Deposited as two major deltaic successions in a restricted marine environment. See also p64-p65, p67-p69, p71, p79.||South Perth Supersequence|Includes the Gage Lowstand Fan.|Conformably overlies the South Perth Sequence 1 and the Parmelia Group (conformably to angular). Overlain conformably by the South Perth Sequence 3.|Fine-grained to granular feldspathic sandstone interbedded with micaceous mudstone and siltstone overlain by an argillaceous micaceous mudstone interbedded with carbonaceous, argillaceous and micaceous siltstone grading to sandstone.|
80800|South Perth Sequence 3|71958|2|Defined|p51, p55-p56, p59-60, p62, p64-p65, p80|Hauterivian|Hauterivian|Vlaming Sub-basin. Named for the South Perth Shale and Supersequence. The type locality is found in Marri 1 (-31.744767, 115.356875) in the interval between 777.2 and 548.5m (total thickness of 228.7m). Age is derived from the presence of diagnostic microfossils including A. alata and B. Jaegeri Dinocysts. In the southern Vlaming Sub-basin it ranges from predominantly mudstone with trace glauconite and pyrite with minor interbeds or glauconitic, pyritic sandstone to fine-grained glauconitic and pyritic siltstone. This unit is penetrated in all analysed wells  [this volume] and ranges in thickness between 20 to 616.2m. Deposited in environments ranging from pro-delta, shelfal, proximal delta front to fluvio-deltaic.||South Perth Supersequence||Conformably overlies the South Perth Sequence 2. Conformably overlain by the Leederville Supersequence.|Dominantly coarse-grained quartzose sandstone with trace pyrite, mica and glauconite interbedded by thin carbonaceous material with rare coal and siltstone.|
80792|South Perth Supersequence|71958|2|Defined|p38, p40-p41, p45-p46|Hauterivian|Valanginian|Vlaming Sub-basin. The name is derived from the South Perth Shale which is included in this sequence. The type locality is defined in Warnbro 1 (-32.23769, 115.347327) between 1489 and 2117.8m (a total thickness of 628.8m). Spring and Newell (1993) conducted a sequence stratigraphic analysis that found this unit coincides with four depositional sequences. Sequence stratigraphy. Age derived from the presence of diagnostic microfossils assigned to G. mutabilis, K. scrutillinum, P. lowryi, A. alata and B. Jageri. This unit is thickest in the Rottnest Trough, the northern extension of the Peel Arch and the northern Mandurah Terrace. The supersequence is absent where it onlaps the Roe High to the west, the Mandurah Terrace to the east and the Vasse Shelf and Sugarloaf Arch to the south. The maximum drilled thickness was 1326.8m intersected in Mallaloo 1. Deposited as two deltaic successions with some lava flows. See also p49, p51, p53-p56, p60-p61, p67, p77-p78, p87.||Warnbro Megasequence|Includes the South Perth Sequence 1, South Perth Sequence 2 and South Perth Sequence 3.|Overlies the Parmelia Group. Unconformably overlies the Charlotte Supersequence. Overlain by the Leederville Supersequence.|Fine-grained to very coarse feldspathic sandstone with interbedded mudstone and siltstone that is overlain by black argillaceous, micaceous mudstone that grades upwards to siltstone with minor sandstone interbeds.|
68645|South Whundo Monzogranite|63441|2|Defined|p10 Tb. 2|Archean|Archean|Of the Orpheus Supersuite. Unconformably overlain by Hardey Formation. Intrudes Nallana Formation. Age: 3013+/-4Ma. Geological province: Pilbara Craton.||||||07-FEB-11
68645|South Whundo Monzogranite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Orpheus Supersuite. Geological province: Pilbara Craton.  Massive, medium- to coarse-grained monzogranite; metamorphosed.||||||07-NOV-08
68645|South Whundo Monzogranite|64580|4|Described|map legend||Mesoarchean|Of Orpheus Supersuite. Massive, medium- to coarse-grained monzogranite; metamorphosed.||||||15-DEC-08
68645|South Whundo Monzogranite|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Orpheus Supersuite.|||Massive, medium- to coarse-grained monzogranite; metamorphosed|
68645|South Whundo Monzogranite|70775|5|Briefly described|p37, p46, p50, p74|Mesoarchean|Mesoarchean||3013 +/- 4 Ma (Smith et al., 1998)|||||
68645|South Whundo Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
68645|South Whundo Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|De Grey Superbasin.|3013+/-4 Ma.|Orpheus Supersuite|||Monzogranite; massive, medium- to coarse-grained; metamorphosed.|
79200|Southern Hills Suite|70182|4|Described|p9, p33-34, p38, p40-41, p43-47|Mesoproterozoic|Mesoproterozoic|New name, after Southern Hills Station. East Albany-Fraser Orogen. Refers to Recherche Supersuite granites with SiO2 > 72 wt%, and typically with notable depletions in HFSE, REE, Th and U compared with other granites of the Supersuite at similar silica values. Geochemistry detailed; magmatic evolution discussed.|c.1320 Ma - 1287 Ma.|Recherche Supersuite.|||Generally leucocratic, weakly peraluminous syenogranites.|13-APR-18
79200|Southern Hills Suite|70735|6|Mentioned|p29, 43 Fig.18|||Albany-Fraser Orogen. Local anatectic melts of Arid Basin metasedimentary rocks.|||||Typically peraluminous syenogranites.|
79200|Southern Hills Suite|70802|4|Described|250k_pre_mesozoic_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen. Events: Albany-Fraser Orogeny Stage I (1330-1260 Ma);  Albany-Fraser Orogeny (1330-1140 Ma); Albany-Fraser Orogeny Stage II (1225-1140 Ma). Magmatism coinciding with Stage I Albany-Fraser Orogeny (Spaggiari et al., 2014). Typically foliated or gneissic, and metamorphosed to amphibolite or granulite facies during either Stage I or II (or both) Albany-Fraser Orogeny (Spaggiari et al., 2014). Sample GSWA 194786 (bt monzogranite) yielded a weighted mean 207Pb*/206Pb* date of 1320+\-8 Ma, interpreted as the magmatic crystallization age of the monzogranite; and concordia age of 1198+\-7 Ma, interpreted as age if high-grade metamorphism. Sample GSWA 194883 (metasyenogranite) yielded a concordia age of 1322+\-12 Ma, interpreted as magmatic crystallisation age of the syenogranite. See also geochron files.|1305+\-2 Ma; 1288+\-3 Ma |Unit of Recherche Supersuite.|||Syenogranite gneiss, typically interlayered with metagabbro|
79200|Southern Hills Suite|70813|5|Briefly described|p6|||||Recherche Supersuite|||Peraluminous syenogranites.|
79200|Southern Hills Suite|71270|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage II (1225 - 1140 Ma); Albany-Fraser Orogeny (1330 - 1140 Ma); Albany-Fraser Orogeny Stage I (1330 - 1260 Ma). See 500k_interpgeop16_lut.csv, 2_5m_interpg|1305+\-2 Ma; 1288+\-3 Ma|Unit of Recherche Supersuite.||Intruded by Esperance Supersuite.|Syenogranite gneiss, typically interlayered with metagabbro|
79200|Southern Hills Suite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Albany-Fraser Orogen.|Max age 1305+/-2 Ma, min 1288+/-3 Ma.|Recherche Supersuite||Locally forms net-veined complexes with Esperence Supersuite units.|Syenogranite gneiss, typically interlayered with metagabbro.|
79200|Southern Hills Suite|72059|5|Briefly described|p67|Ectasian|Ectasian|Geological province: Fraser Zone, Albany-Fraser Orogen.||Unit of Recherche Supersuite.||||
79200|Southern Hills Suite|72710|5|Briefly described|p9.|Ectasian|Ectasian|One of two geochemically distinct suites that form the Recherche Supersuite. Source components include Archean, Paleoproterozoic and Mesoproterozoic rocks.|1330 Ma to 1276 Ma.|Recherche Supersuite|||Includes metabasalts and metagabbros.|
37148|Spear Hill Monzogranite|23755|5|Briefly described|p18 Table 2|Archean|Archean|||||||07-NOV-08
37148|Spear Hill Monzogranite|23783|5|Briefly described|p115 Fig. 64|Archean|Archean|||||||07-NOV-08
37148|Spear Hill Monzogranite|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Age: 2851+/-2Ma (Nelson, 1998).  Geological Province: Pilbara Craton.||||||07-NOV-08
37148|Spear Hill Monzogranite|24110|5|Briefly described|Plate 1|Archean|Archean|Belongs to Shaw Granitoid Complex.  Geological Province: Pilbara Craton||||||07-NOV-08
37148|Spear Hill Monzogranite|24185|5|Briefly described|p750|Archean|Archean|Age: ca. 2851 +/- 2 Ma (U-Pb zircons, Nelson, 1998) Geological Province: Pilbara Craton.||||||07-NOV-08
37148|Spear Hill Monzogranite|24193|5|Briefly described|p877 Tb.1|Archean|Archean|Geological Province: Pilbara Craton. Of the Shaw granitoid complex.||||||07-NOV-08
37148|Spear Hill Monzogranite|24531|5|Briefly described|p8-9 Fig. 3|Archean|Archean|Of the Shaw Granitoid Complex.  Age: 2851+/-2Ma (Nelson, 1998).||||||07-NOV-08
37148|Spear Hill Monzogranite|24532|5|Briefly described|Map legend|Archean|Archean|Of the Shaw Granitoid Complex. Age: c. 2851Ma.||||||15-APR-13
37148|Spear Hill Monzogranite|50427|5|Briefly described|p186|Archean|Archean|Of Shaw Granitoid Complex.||||||07-NOV-08
37148|Spear Hill Monzogranite|61252|6|Mentioned|p67 Tb.1|||Of the Shaw granitoid complex.||||||
37148|Spear Hill Monzogranite|63441|5|Briefly described|p12 tb. 2|Archean|Archean|Of Split Rock Supersuite. Age: 2851+/-2Ma. Geological province: Pilbara Craton.||||||07-FEB-11
37148|Spear Hill Monzogranite|66108|5|Briefly described|Map legend|Neoarchean|Neoarchean|Unit in Split Rock Supersuite. c. 2851 Ma. Coarse-grained to K-feldspar-porphyritic biotite monzogranite.||||||15-APR-13
37148|Spear Hill Monzogranite|68282|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|c.2851 Ma|Of the Split Rock Supersuite|||Coarse-grained to K-feldspar-porphyritic biotite monzogranite.|
37148|Spear Hill Monzogranite|69015|5|Briefly described|Map Legend|||Pilbara Craton.||Of the Split Rock Supersuite.|||Coarse-grained to K-feldspar porphyritic biotite monzogranite.|02-MAY-14
37148|Spear Hill Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Coarse-grained to K-feldspar porphyritic biotite monzogranite.|
37148|Spear Hill Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; Split Rock Supersuite Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|2851 Ma (isotopic)|Unit of Split Rock Supersuite.|||Coarse-grained to K-feldspar porphyritic biotite monzogranite|
37148|Spear Hill Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
37148|Spear Hill Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||2851+/-2 Ma|Split Rock Supersuite|||Coarse-grained to K-feldspar porphyritic biotite monzogranite.|
26904|Spearhole Formation|22589|6|Mentioned|p125||Proterozoic|||||||
26904|Spearhole Formation|22816|5|Briefly described|p8 Table 1|||Savory Group.||||||11-APR-08
26904|Spearhole Formation|22901|6|Mentioned|76 fig 2|||Geol province Officer Basin||||||
26904|Spearhole Formation|22907|6|Mentioned|41|||Geol province Officer Basin. Parent Sunbeam Group||||||
26904|Spearhole Formation|23156|4|Described|p16|Neoproterozoic|Neoproterozoic|For location of type area see p16.||||||
26904|Spearhole Formation|23557|5|Briefly described|p95 Fig.1|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||
26904|Spearhole Formation|24161|6|Mentioned|p29|||||||||
26904|Spearhole Formation|24246|5|Briefly described|p17|Cambrian|Proterozoic|Overlain by Mundadjini Formation. Geological Province: Savory Basin.||||||
26904|Spearhole Formation|24390|5|Briefly described|p12 Table 3|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
26904|Spearhole Formation|42708|5|Briefly described|Plate 1|Proterozoic||Reserved as Spearhole.||||||
26904|Spearhole Formation|43209|5|Briefly described|map legend||Neoproterozoic|Of Savory Group.||||||
26904|Spearhole Formation|43229|5|Briefly described|Map Legend||Neoproterozoic|Of Savory Group.||||||11-APR-08
26904|Spearhole Formation|43492|3|Fully described|9|||Formerly Calyie Sandstone.||||||11-APR-08
26904|Spearhole Formation|43756|6|Mentioned|Fig.1,p535|||||||||
26904|Spearhole Formation|50008|5|Briefly described|p46 Fig.3|Neoproterozoic||Of Sunbeam Group. Geological Province: Officer Basin.||||||
26904|Spearhole Formation|50085|5|Briefly described|p12 Tb. 3|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
26904|Spearhole Formation|61023|5|Briefly described|p16 Tb. 3|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||11-APR-08
26904|Spearhole Formation|61716|6|Mentioned|p642|||Overlain by the lower Mundadjini member (Mundadjini Formation). Geological Province: Officer Basin.||||||
26904|Spearhole Formation|61732|5|Briefly described|p4 Fig. 3, p58 Fig. 22|Willouran|Willouran|Of the Sunbeam Group. May have faulted contact with Boondawari Formation. Geological Province: northwestern Officer Basin.||||||07-FEB-11
26904|Spearhole Formation|62453|3|Fully described|p5 Fig. 3, 22, 54|Cryogenian|Cryogenian|Of the Sunbeam Group. Geological Province: Officer Basin. Overlies Brassey Range Formation. Sandstone, conglomerate and siltstone. Thickness: up to 1000m. Disconformably overlain by Mundadjini Formation.||||||
26904|Spearhole Formation|62987|5|Briefly described|p30|Neoproterozoic|Neoproterozoic|Of the Sunbeam Group. Geological Province: Officer Basin.||||||
26904|Spearhole Formation|64580|4|Described|map legend||Neoproterozoic|Of Sunbeam Group.  Sandstone, in part pebbly, siltstone, and local conglomerate lenses.||||||09-DEC-08
26904|Spearhole Formation|64772|5|Briefly described|p15, Plate 1|Neoproterozoic|Neoproterozoic|Of the Sunbeam Group. Geological province: Officer Basin, Centralian Superbasin. Shown adjacent to Tarcunyah Group in Plate 1. ?lateral equivalent. Sandstone, in part pebbly, siltstone, and local conglomerate lenses. See also||||||25-NOV-13
26904|Spearhole Formation|64793|6|Mentioned|p283 fig 2, p285 Fig.4|Cryogenian|Cryogenian|Of NW Officer Basin.||||||
26904|Spearhole Formation|64970|6|Mentioned|p719 Fig. 2|Riphean|Riphean|Geological Province: Officer Basin.||||||27-MAY-09
26904|Spearhole Formation|65363|6|Mentioned|p5 Fig.4. |Neoproterozoic|Neoproterozoic|||||||
26904|Spearhole Formation|65365|5|Briefly described|p10 Fig. 4|Cryogenian|Cryogenian|Northwestern Officer Basin||||||
26904|Spearhole Formation|65366|5|Briefly described|p23 Fig. 3|Cryogenian|Cryogenian|Northwestern Officer Basin||||||
26904|Spearhole Formation|65410|6|Mentioned|p72.|Neoproterozoic|Neoproterozoic|Savory Basin. Arenaceous. Part of Supersequence 1.||||||
26904|Spearhole Formation|65416|5|Briefly described|p137, p140, p145.|Neoproterozoic|Neoproterozoic|Officer Basin. Part of Sequence LP1B of Supersequence PL1. Correlated with Browne Formation on bases of lithostratigraphy, depositional environments and underlying unconformities. High-energy braided stream environment.||||Unconformably overlies Jilyili Formation.|Coarse- to medium-grained sandstones with scattered pebbles and interbedded pebbly conglomerate.|
26904|Spearhole Formation|67195|5|Briefly described|p10 fig 6, p19 table 1, p40, p45, 48|Neoproterozoic|Neoproterozoic|Savory area, western Officer Basin. Thermal conductivity of 3.54 W/mK. Basal unit of one well in this study. See also App 1, App 2.||||Overlies Brassey Range Formation. Overlain by Mundadjini Formation.|Coarse-grained to granular red sandstone; red siltstone; red siltstone/claystone.|04-JAN-23
26904|Spearhole Formation|67200|5|Briefly described|app 2 p10||||||||Sandstone, siltstone and claystone.|
26904|Spearhole Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|NW Officer Basin.||||||
26904|Spearhole Formation|69185|4|Described|500k_geologyp08_lut.csv||Neoproterozoic|Of Officer Basin.||Unit of Sunbeam Group.|||Undivided; sandstone, in part pebbly, siltstone, and local conglomerate lenses|
26904|Spearhole Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, conglomerate, siltstone|
78611|Speedway Andesite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2692 - 2655 Ma (inferred).|Black Flag Group|||Andesite; pale grey, coherent to brecciated; microporphyritic; ubiquitous fine biotite-hornblende mafic inclusions; metamorphosed. Breccia dominated by andesitic clasts; diffuse bedding; moderately sorted; metamorphosed|
78611|Speedway Andesite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2692-2655 Ma (inferred)|Unit of Black Flag Group.|||Andesite; pale grey, coherent to brecciated; microporphyritic; ubiquitous fine biotite-hornblende mafic inclusions; metamorphosed; Breccia dominated by andesitic clasts; diffuse bedding; moderately sorted; metamorphosed.|
80969|Speewah Basin felsic extrusive unit 80969|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Informal unit. Speewah Basin. Age inferred.|||||Porphyritic dacite; fine-grained, massive or flow banded.|
81034|Splinter Gneiss|70802|4|Described|250k_pre_mesozoic_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen. Events: Albany-Fraser Orogeny Stage I (1330-1260 Ma);  Albany-Fraser Orogeny (1330-1140 Ma); Albany-Fraser Orogeny Stage II (1225-1140 Ma).|1276+\-6 Ma|Unit of Recherche Supersuite.|||Gabbro gneiss, locally garnet-rich, and layered intermediate gneiss; contains intrusions of Esperance Supersuite monzogranite and pegmatite|
81034|Splinter Gneiss|71270|4|Described|500k_interpgeop16_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage II (1225 - 1140 Ma); Albany-Fraser Orogeny (1330 - 1140 Ma); Albany-Fraser Orogeny Stage I (1330 - 1260 Ma).|1276+\-6 Ma|Unit of Recherche Supersuite.|||Gabbro gneiss, locally garnet-rich, and layered intermediate gneiss; contains intrusions of Esperance Supersuite monzogranite and pegmatite|
81034|Splinter Gneiss|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Albany-Fraser Orogen.|1276+/-6 Ma.|Recherche Supersuite|||Gabbro gneiss, locally garnet-rich, and layered intermediate gneiss; contains intrusions of Esperance Supersuite monzogranite and pegmatite.|
68672|Split Rock Supersuite|61253|5|Briefly described| p52 Fig. 2|Archean|Archean|Age: 2880-2830Ma. Geological Province: Pilbara Craton. See also p54-55 Fig. 3.||||||16-APR-13
68672|Split Rock Supersuite|63417|5|Briefly described|Map legend|Archean|Archean|Includes Mondana and Cookes Creek Monzogranites, Bonney Downs Granite and Moolyella Monzogranite. Geological Province: Pilbara Craton.||||||07-NOV-08
68672|Split Rock Supersuite|63420|5|Briefly described|Map legend|Archean|Archean|Includes Thelman Monzogranite, Tabba Tabba Leucogranite, Poocatche Monzogranite, Myanna Leucogranite, Minnamonica, Kimmys Bore and Kadgewarrina Monzogranites. Geological Province: Pilbara Craton.||||||07-NOV-08
68672|Split Rock Supersuite|63441|4|Described|p38, p12 tb. 2|Archean|Archean|Contains 12 named monzogranites and Myanna Leucogranite. Age: 2890-2830Ma. Highly fractionated, post-tectonic Sn-Ta-Li-Be-bearing monzogranite to syenogranite plutons and pegmatites. Geol. Prov: East Pilbara and Kurrana Terranes. See also p34 Fig. 13.||||||16-APR-13
68672|Split Rock Supersuite|63538|6|Mentioned|p6 Fig. 3|Archean|Archean|Geological Province: Pilbara Craton.||||||19-APR-13
68672|Split Rock Supersuite|63854|6|Mentioned|p230|Mesoarchean|Mesoarchean|North Pilbara Craton. Characterized by post-tectonic tin-tantalum-lithium-beryl-bearing granitic rocks, typically with pronounced radiometric signatures.|c.2890-2830 Ma||Includes Bonney Downs Granite.|||
68672|Split Rock Supersuite|64580|4|Described|map legend||Mesoarchean|||||||
68672|Split Rock Supersuite|64621|5|Briefly described|Map legend|Archean|Archean|Includes the Moolyella Monzogranite. Age: 2839-2831Ma.||||||07-NOV-08
68672|Split Rock Supersuite|64656|5|Briefly described|Map Legend|Archaean|Archaean|Includes Bonney Downs Granite. Geological Province: Pilbara Craton.||||||
68672|Split Rock Supersuite|64728|6|Mentioned|p97.|||||Unit in Pilbara granite-greenstone terrane.||||
68672|Split Rock Supersuite|65008|6|Mentioned|p21|Mesoarchean|Mesoarchean|Characterised by pronounced radiometric signatures. See Split Rock Suite in this paper.|2890-2830 Ma||Includes the Bonney Downs Granite.||Characterised by tin-tantalum-lithium-beryl bearing granitic rocks.|
68672|Split Rock Supersuite|65727|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Pilbara Craton.|||Includes Mondana and Moolyella Monzogranites.|||
68672|Split Rock Supersuite|65825|4|Described|p12.|Archean|Archean|A group of late- to post-tectonic Sn-Ta-Li-bearing monzogranites ('tin granites') emplaced across East Pilbara Granite-Greenstone Terrane and Kurrana Terrane at 2.89 - 2.83 Ga. Has a distinct radiometric signature: high K, U and Th counts. Extremely weathered. Is largely undeformed to the west.|2861 +/- 4 Ma to 2836 +/- 6 Ma (Nelson 2005).||Includes Bonney Downs Granite.|Interleaved with Golden Eagle Orthogneiss. Is faulted against the Coondamar Formation.|Strongly deformed, fine- to medium-grained, weakly porphyritic monzogranite with local pegmatite zones and sparse aplite veins.|
68672|Split Rock Supersuite|65827|4|Described|p1, p6 Tb.2, p9 Fig 3, p15-16, p29|Mesoarchean|Mesoarchean|2890-2830 Ma. Of Mount Edgar Granitic Complex and Corunna Downs Granitic Complex; monzogranite. Includes Moolyella Monzogranite, Mondana Monzogranite. Intrudes Cleland Supersuite.||||||
68672|Split Rock Supersuite|66108|5|Briefly described|Map legend|Neoarchean|Neoarchean|Pilbara Craton. Comprises Tambourah, Spear Hill, Poocatche, Numbana, Moolyella, Mondana, Minnamonica, Gillam and Cooglegong Monzogranites; and a mapped but unnamed unit of weakly metamorphosed monzogranite, syenogranite and pegmatite.||||||
68672|Split Rock Supersuite|66118|6|Mentioned|p148 Fig.2|||Pilbara Craton. East Pilbara Terrane.|c. 2850 Ma|||||
68672|Split Rock Supersuite|66217|5|Briefly described|p1, p9, p11. |Mesoarchean|Mesoarchean|Post-tectonic granitic rocks intruding the Kurrana and East Pilbara Terranes. Probable source of alluvial Sn, Ta and Li in the Warralong and Marble Bar greenstone belts.|2.89-2.83 Ga.|Unit in Carlindi Granitoid Complex.|Includes Moolyella Monzogranite.||Undeformed monzogranites and syenogranites.|
68672|Split Rock Supersuite|67201|5|Briefly described|p5, p7 Fig.4, p19, p22 Fig.13, p24|Archean|Archean|In northern Pilbara Craton, West Pilbara Superterrane and East Pilbara Terrane. In De Grey Superbasin.|2890-2830 Ma||||Virtually unfoliated syenogranite and monzogranite. Highly fractionated, Sn-Ta-Li bearing, post-tectonic monzogranites.|
68672|Split Rock Supersuite|68035|5|Briefly described|p291, 294, p287, p286 Fig 3|Mesoarchean|Mesoarchean|Emplaced in a SE-NW-trending linear belt across the Kurrana and East Pilbara terranes between 2.89 - 2.83 Ga (Van Kranendonk et al., 2007a). Includes pegmatite-hosted Sn-Ta deposits around the margins of highly fractionated post-orogenic granites.|2890 - 2830 Ma||||Highly fractionated, Sn-Ta-Li bearing, post-orogenic monzogranites.|
68672|Split Rock Supersuite|68280|6|Mentioned|p3|Mesoarchean|Mesoarchean||2890-2830 Ma|||||
68672|Split Rock Supersuite|68281|5|Briefly described|Map Legend|Neoarchean|Mesoarchean|Pilbara Craton. Minimum age from cross-cutting dykes.|||Includes Kimmys Bore Monzogranite, Kadgewarrina Monzogranite, Minnamonica Monzogranite.|Is intruded by dykes of Black Range Dolerite Suite.|Monzogranites.|23-SEP-13
68672|Split Rock Supersuite|68282|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|||Includes Cooglegong Monzogranite, Spear Hill Monzogranite, Tambourah Monzogranite.||Monzogranites.|
68672|Split Rock Supersuite|68283|5|Briefly described|Map Legend|Archean|Archean|Pilbara Craton.|||Includes Kadgewarrina, Kimmys Bore, Minnamonica, Poocatche and Thelman Monzogranites; Myanna and Tabba Tabba Leucogranites.||Monzogranites; minor granite and pegmatite.|19-JUN-14
68672|Split Rock Supersuite|69012|5|Briefly described|Map Legend|Archean|Archean||||Includes the Cooglegong Monzogranite and Mondana Monzogranite.|||
68672|Split Rock Supersuite|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton. Also includes 3 unnamed facies mapped separately.|||Includes Gillam, Minnamonica, Numbana and Poocatche Monzogranites.|Parts form pods and larger bodies in the Paleoarchean Motherin Monzogranite, implying Intrudes Motherin Monzogranite?|Undivided granitic rocks including monzogranite, syenogranite and pegmatite.|16-NOV-16
68672|Split Rock Supersuite|69015|5|Briefly described|Map Legend|Neoarchean|Mesoarchean|Pilbara Craton. Includes 1 unnamed sub-unit.|||Includes the Spear Hill Monzogranite.||Seriate to porphyritic biotite leucogranite, massive to weakly foliated, metamorphosed; coarse-grained to K-feldspar porphyritic biotite monzogranite.|02-MAY-14
68672|Split Rock Supersuite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|Also includes Cooglegong Monzogranite, Gillam Monzogranite, Kimmys Bore Monzogranite, Kadgewarrina Monzogranite, Minnamonica Monzogranite, Mondana Monzogranite, Numbana Monzogranite,Poocatche Monzogranite, Tambourah Monzogranite, Thelman Monzogranite, Tabba Tabba Leucogranite, Spear Hill Monzogranite, Myanna Leucogranite/|||Includes Moolyella Monzogranite, Bonney Downs Monzogranite, Cookes Creek Monzogranite||Undivided granitic rocks including monzogranite, syenogranite, and pegmatite. Biotite and muscovite-biotite monzogranite, massive to weakly foliated. Seriate to porphyritic biotite leucogranite; massive to weakly foliated, pegmatite.|
68672|Split Rock Supersuite|69185|5|Briefly described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.|||Includes Cookes Creek Monzogranite, Moolyella Monzogranite, Numbana Monzogranite.|||
68672|Split Rock Supersuite|69301|4|Described|p4, p5 Fig.3, p16, p23|||Pilbara Craton. West Pilbara Superterrane and East Pilbara Terrane. Posttectonic granitic intrusions that were emplaced after Pilbara-wide orogeny (2.94 to 2.90 Ga). |2.89-2.83 Ga|||Intrudes East Pilbara and Kurrana Terranes and eastern part of Mallina Basin.|A supersuite of highly fractionated, post-orogenic granites; mainly as almost horizontal sheets of monzogranite and syenogranite, with peripheral swarms of horizontal and low-dipping pegmatite veins.|
68672|Split Rock Supersuite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; Split Rock Supersuite Event. Also includes MONZOGRANITES: Bonney Downs, Cooglegong, Cookes Creek, Gillam, Kadgewarrina, Kimmys Bore, Minnamonica, Mondana, Moolyella, Numbana, Poocatche, Spear Hill, Tambourah, Thelman. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|2851-2831 Ma (inferred)||Includes LEUCOGRANITES; Myanna, Tabba Tabba.||Biotite-, biotite-muscovite and muscovite-biotite monzogranite; biotite leucogranite, undivided granitic rocks including monzogranite, syenogranite, and pegmatite.|
68672|Split Rock Supersuite|70022|6|Mentioned|p115|||Pilbara Craton.||||||
68672|Split Rock Supersuite|70775|4|Described|iii, iv, p1, p5-p9, p18|Mesoarchean|Mesoarchean|Together with the Sisters Supersuite forms the Pippingarra Granitic Complex. Intrusions of this supersuite were emplaced along a wide northwest-trending belt across the northern Pilbara Craton. See also p42, p44 fig 27, p71, p80-p81.|c. 2851-2831 Ma||Includes the Myanna Leucogranite, Tabba Tabba Leucogranite and Thelman Monzogranite.||Highly fractionated monzogranites.|
68672|Split Rock Supersuite|70826|6|Mentioned|p8|Mesoarchean|Mesoarchean|||||||
68672|Split Rock Supersuite|70884|6|Mentioned|p122|Mesoarchean|Mesoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|c. 3.2-2.83 Ga|||||
68672|Split Rock Supersuite|71041|5|Briefly described|p45 fig 2, p47 fig 4, p42|Mesoarchean|Mesoarchean||2890-2830 Ma||Includes the Numbana Monzogranite.|||10-NOV-17
68672|Split Rock Supersuite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||syenogranite, monzogranite, felsic gneiss, pegmatite|
68672|Split Rock Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Includes Moolyella, Cookes Creek, Bonney Downs, Spear Hill, Cooglegong, Gillam, Kimmys Bore, Kadgewarrina, Minnamonica, Mondana Monzogranites, Myanna Leucogranite, Numbana, Poocatche, Tambourah, Thelman Monzogranites, Tabba Tabba Leucogranite.|max age 2851+/-2 Ma, min 2831+/-11 Ma||Includes 16 named units and one unnamed monzogranite. See Comments field for full list.||Undivided granitic rocks including monzogranite, syenogranite, and pegmatite; Biotite(-muscovite) monzogranite; equigranular to weakly K-feldspar porphyritic; locally highly leucocratic and ghost-banded; massive to weakly foliated.|
68672|Split Rock Supersuite|72251|5|Briefly described|p54|||Geological province: East Pilbara Terrane and West Pilbara Superterrane, Pilbara Craton.||||Underlain by Cutindina Supersuite or Sisters Supersuite.||
68672|Split Rock Supersuite|72668|5|Briefly described|p4, p17-19|||Emplaced in a NW-SE trending linear belt across the Kurrana Terrane-East Pilbara boundary. Geochemistry is discussed.|c. 2890-2830 Ma||||Highly fractionated, Sn-Ta-Li bearing monzogranites.|
68672|Split Rock Supersuite|73598|6|Mentioned|p1212|Mesoarchean|Mesoarchean|East Pilbara Terrane.||||||
74795|Spring Camp Formation|65545|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Mount James Subgroup, Pooranoo Metamorphics, Gascoyne Province.  c. 1680 Ma. Quartz and quartz-muscovite schist; foliated; quartz metasandstone; feldspathic metasandstone and quartz-lithic metasandstone; locally ripple-marked and cross-bedded.||||||
74795|Spring Camp Formation|65549|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Mount James Subgroup, Pooranoo Metamorphics. Overlies Quartpot Pelite, underlies Yilgatherra Formation. Quartzite and quartz-muscovite schist; quartz metasandstone, feldspathic metasandstone, and quartz-lithic metasandstone.||||||
74795|Spring Camp Formation|66110|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Mount James Subgroup. Aged 1782-1677 Ma. Quartzite and quartz-muscovite schist; foliated; quartz metasandstone, feldspathic metasandstone, and quartz-lithic metasandstone; locally ripple marked and cross-bedded.||||||
74795|Spring Camp Formation|66299|4|Described|p51, pp215-237, p328.|Paleoproterozoic|Paleoproterozoic|Deposited in shallow-marine to inter-tidal environment. Deformed by Edmundian Orogeny between c.1026 Ma and c.995 Ma.|1782 +/- 5 Ma to c.1680 Ma.|Upper unit in Mount James Subgroup.||Overlies Biddenew Formation. Locally unconformably overlies Moorarie Supersuite and Leake Spring Metamorphics.|Quartzite and quartz-muscovite schists; foliated; quartz metasandstone, feldspathic metasandstone, and quartz-lithic metasandstone; locally ripple marked and cross-bedded.|
74795|Spring Camp Formation|66579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Unit in Mount James Subgroup.|||Quartzite and quartz-muscovite schist; foliated; quartz metasandstone, feldspathic metasandstone and quartz-lithic metasandstone; locally ripple-marked and cross-bedded.|
74795|Spring Camp Formation|66950|6|Mentioned|p12|||||Of the Mount James Subgroup.||||
74795|Spring Camp Formation|67247|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.||Unit in Mount James Subgroup.|||Quartzite and quartz-muscovite schist; foliated; quartz metasandstone, feldspathic metasandstone, and quartz-lithic metasandstone; locally ripple-marked and cross-bedded.|
74795|Spring Camp Formation|67371|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.|1782 - 1677 Ma.|Unit in Mount James Subgroup.|||Quartzite and quartz-muscovite schist; foliated; quartz metasandstone, feldspathic metasandstone, and quartz-lithic metasandstone; locally ripple-marked and cross-bedded.|
74795|Spring Camp Formation|68521|5|Briefly described|Map Legend|Statherian|Statherian|Geochronology from Sheppard et al. (2005).|c.1680 Ma|Of the Mount James Subgroup.|||Quartzite and quartz-muscovite schist; foliated; quartz metasandstone, feldspathic metasandstone, and quartz-lithic metasandstone; locally ripple marked and cross-bedded.|
74795|Spring Camp Formation|68522|5|Briefly described|Map Legend|Statherian|Statherian|Gascoyne Province.|1760-1680 Ma|Of the Mount James Subgroup.|||Quartzite and quartz-muscovite schist; foliated; quartz metasandstone, feldspathic metasandstone, and quartz-lithic metasandstone; locally ripple marked and cross-bedded.|
74795|Spring Camp Formation|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Age derived from samples of quartzite (191994.1.pdf, 185954.1.pdf) and constrain maximum age of sedimentary protoliths.|1787 +/- 12 Ma  1807 Ma  (SHRIMP)|Mount James Subgroup||Conformably overlies Biddenew Formation, unconformably overlain by Edmund Group|Quartzite and quartz--muscovite schist; foliated; quartz metasandstone, feldspathic metasandstone, and quartz-lithic metasandstone; locally ripple marked and cross-bedded|
74795|Spring Camp Formation|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 185953.1.pdf|1758-1683 Ma|Mount James Subgroup||Conformably overlies Biddenew Formation, Unconformably overlain by Edmund Group, intruded by Durlacher Supersuite|Quartzite and quartz--muscovite schist; foliated; quartz metasandstone, feldspathic metasandstone, and quartz-lithic metasandstone; locally ripple marked and cross-bedded.|
31902|Spring Creek intrusion|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
31902|Spring Creek intrusion|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31902|Spring Creek intrusion|63866|5|Briefly described|p131|Orosirian|Orosirian|Central Zone, Halls Creek Orogen.|c. 1845-1830 Ma||||Ultramafic-mafic plutonic rocks.|
31902|Spring Creek intrusion|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Layered mafic-ultramafic intrusions; peridotite, troctolite, gabbro, olivine gabbro, gabbronorite, magnetite gabbro, magnetite-olivine gabbro, leucogabbro, leucogabbronorite, and anorthosite.||||||
31902|Spring Creek intrusion|69099|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|Grouped as McIntosh, Armanda, and Spring Creek intrusions, with single lith description in 500k_geologyp08_lut.csv. |||||Layered mafic-ultramafic intrusions; peridotite, troctolite, gabbro, olivine gabbro, gabbronorite, magnetite gabbro, magnetite-olivine gabbro, leucogabbro, leucogabbronorite, and anorthosite.|04-AUG-15
31902|Spring Creek intrusion|71113|6|Mentioned|p96|||Geological province: Central Zone, Lamboo Province, Halls Creek Orogen.||||||
31902|Spring Creek intrusion|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Layered mafic-ultramafic intrusion; gabbro, leucogabbro, leucogabbronorite, gabbronorite, anorthosite, minor troctolite; some olivine and/or chromitite-bearing; in rhythmic cycles; peridotite and troctolite|
37894|Spring Well Complex|23930|6|Mentioned|p129 Fig.1|Archean|Archean|See also Spring Well Volcanic complex. Geological Province: Yilgarn Craton.||||||07-NOV-08
37894|Spring Well Complex|24135|3|Fully described|p13|Archean|Archean|||||||07-NOV-08
37894|Spring Well Complex|62107|6|Mentioned|p1391 Fig. 2|||In the Yandal belt.||||||
37894|Spring Well Complex|63980|4|Described|pp63-66, p69.|Archean|Archean|Gindalbie Terrane. Yandal Greenstone Belt, 115 km north of Leonora. c.3 km thick sequence youngs to the west. Facies associations vary markedly in thickness along strike. Probably represents volcanism at continental marginal arc or within a rifted mature island-arc system.  Ages from two different rhyolite samples.|2694 +/- 4 Ma, 2690+/-6 Ma both SHRIMP.||||Calc-alkaline basaltic andesite to andesite, and dacite-rhyolite lavas, associated breccias; abundant microdiorite sills and dykes; subordinate volcanogenic conglomerate, sandstone and shale; high Sr/Y andesite and lamprophyre dykes.|26-SEP-14
37894|Spring Well Complex|65264|5|Briefly described|p19|||Poorly sorted, matrix-supported, lacking in any stratification, and contains a range of volcanic clasts.||||||07-FEB-11
37894|Spring Well Complex|66880|5|Briefly described|p13, p27.|Archean|Archean|Intruded by a dyke swarm dated at 2666 +/- 7 Ma. Geochemically similar to calc-alkalic volcanic and volcaniclastic Kurnalpi Sequence rocks, reflecting similar intra-arc or arc-related basins.|2694 +/- 4 Ma.|||Intruded by porphyritic andesite dykes.|Intermediate calc-alkalic volcaniclastic rocks.|
73570|Springhill Limestone Member|63454|4|Described|p76|Late Pleistocene|Late Pleistocene|See also Springhill Member. Lower part of Kooallup Limestone. Calcilutite and shelly calcilutite. It should be distinguished from the 2-worded Palaeozoic Spring Hill Limestone in Bonapart Basin (Druce 1963).||||||
78622|Springvale Suite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.|||Includes 3 unnamed units.||Leucogabbro, anorthosite, and minor troctolite; olivine gabbro and chromite layers; rhythmic cycles.|04-AUG-15
78622|Springvale Suite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Paperbark Supersuite|||Leucogabbro, anorthosite, troctolite, olivine gabbro and gabbronorite. Chromite layers and peridotite.|
78622|Springvale Suite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone.|1864-1852 Ma (Inferred)||||Leucogabbro, anorthosite, and minor troctolite; olivine gabbro and chromite layers; olivine gabbronorite, troctolite, gabbro, and gabbronorite, peridotite|
78622|Springvale Suite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1857 Ma|Paperbark Supersuite|||Leucogabbro, anorthosite, minor troctolite, olivine gabbro and chromite layers. Olivine gabbronorite, gabbro and gabbronorite. Peridotite.|
78622|Springvale Suite|70812|5|Briefly described|p6, p8, p20, p22, p43|Orosirian|Orosirian|Western Zone of the Halls Creek Orogen, Lamboo Province. No mineral deposits are known in this unit.|c. 1857 Ma||||Layered mafic and ultramafic rocks.|
78622|Springvale Suite|70851|5|Briefly described|p4|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province.|c. 1850 Ma|||||
78622|Springvale Suite|71113|6|Mentioned|p96|||Geological province: Western Zone, Lamboo Province, Halls Creek Orogen.||||||
78622|Springvale Suite|71140|6|Mentioned|p96|||Western Zone, Lamboo Province, Halls Creek Orogen.||||||
78622|Springvale Suite|71267|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma)|1864-1852 (inferred); 1857+\2 Ma (isotopic)||||Leucogabbro, anorthosite, and minor troctolite; olivine gabbro and chromite layers; olivine gabbronorite, troctolite, gabbro, and gabbronorite, peridotite|
78622|Springvale Suite|71873|6|Mentioned|p426|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province.||||||
31796|Springvale intrusion|43854|5|Briefly described|Map Legend||Proterozoic|Variation on Springvale Complex?||||||
31796|Springvale intrusion|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31796|Springvale intrusion|60498|5|Briefly described|p1016 Fig.1, pp1017-1018, pp1020-1025.|Paleoproterozoic|Paleoproterozoic|Over 2 km thick; its geochemistry is dealt with in detail in this study, particularly halogens in apatites and biotites. Intrusions form dipping sheets. Weak concentrations of Ni, Cu, Cr, PGE mineralisation. |1857 +/- 2 Ma (Page & Hoatson 2000).||||Layered mafic-ultramafic intrusion: olivine gabbro, olivine gabbronorite, gabbro, troctolite, anorthositic gabbro, lherzolite.|03-JAN-18
31796|Springvale intrusion|63866|4|Described|p133, p138|Orosirian|Orosirian|Western Zone, Halls Creek Orogen. Numeric age is derived from the leucogabbro component of this unit and is interpreted as the emplacement age.|c. 1857 Ma (Page and Hoatson, 2000)|||Intrudes the Paperbark Supersuite.|Olivine gabbro, gabbronorite, troctolite, leucogabbro and anorthosite.|
31796|Springvale intrusion|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Layered mafic-ultramafic intrusions; peridotite, troctolite, gabbro, olivine gabbro, olivine gabbronorite, gabbronorite, leucogabbro, and anorthosite; minor chromitite layers.||||||15-DEC-08
31796|Springvale intrusion|69003|5|Briefly described|p22|Paleoproterozoic|Paleoproterozoic|E Kimberley region, Halls Creek Orogen. Hosts minor Ni-Cu-PGE and associated chromite.|1857 +/- 2 Ma.|||||
31796|Springvale intrusion|69099|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|Replaced by Springvale Suite? Grouped as Springvale, Wilagee, and Foal Creek intrusions, with a single lith description in 500k_geologyp08_lut.csv.|||||Layered mafic-ultramafic intrusions; peridotite, troctolite, gabbro, olivine gabbro, olivine gabbronorite, gabbronorite, leucogabbro, and anorthosite; minor chromitite layers.|04-AUG-15
31796|Springvale intrusion|69634|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|Grouped with Wilagee and Foal Creek intrusions.|||||Layered mafic-ultramafic intrusions; peridotite, troctolite, gabbro, olivine gabbro, olivine gabbronorite, gabbronorite, leucogabbro, and anorthosite; minor chromitite layers.|
31796|Springvale intrusion|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Layered mafic-ultramafic intrusion; gabbro, leucogabbro, leucogabbronorite, gabbronorite, anorthosite, minor troctolite; some olivine and/or chromitite-bearing; in rhythmic cycles; peridotite and troctolite|
81268|Stafford Suite|70554|6|Mentioned|p799|Paleoproterozoic|Paleoproterozoic|Geologial province: Aileron province? See also Stafford Event p798.|1815-1795 Ma|||||07-AUG-19
23987|Stag Arrow Formation|23594|6|Mentioned|p20|||Underlying unit Woblegun Formation.||||||
23987|Stag Arrow Formation|24183|5|Briefly described|p21|||Of the Manganese Subgroup. Equivalent to the Backdoor Formation. Geological Province: Bangemall Basin.||||||
23987|Stag Arrow Formation|41669|2|Defined|Table 5|Precambrian?||Fully described p38.||||||28-MAY-19
23987|Stag Arrow Formation|41768|4|Described|p38|||See also Table 1||||||
23987|Stag Arrow Formation|43055|3|Fully described|Table 4, Table 5|||of Manganese Group||||||
23987|Stag Arrow Formation|43056|5|Briefly described|Map Legend|||of Manganese Group||||||
23987|Stag Arrow Formation|44142|5|Briefly described|p315-316 Tb.4-4, p322-323, p324|||Widespread unit. 500-1500m thick marine shelf/barrier bar deposits with stromatolites. Upper interbedded sandstone-shale unit host to enigmatic bedding-plane structures (illustrated), possibly megascopic algae.||Manganese Subgroup||Overlies Woblegun Formation conformably. Overlain conformably by Enacheddong Dolomite.|Dominantly medium-grained sandstone, locally interbedded with siltstone, shale, conglomerate, dolomite, locally abundant; minor chert, glauconitic sandstone.|13-MAR-18
23987|Stag Arrow Formation|60535|5|Briefly described|p556|Mesoproterozoic|Mesoproterozoic|Of the Manganese Group (Bangemall Formation).||||||
23987|Stag Arrow Formation|65830|6|Mentioned|p18|||Contains horizons with the same 'strings of beads' megafossils that occur in the Backdoor Formation (Collier Group).||Of the Manganese Group.||Correlated with Backdoor Formation.||
23987|Stag Arrow Formation|66107|5|Briefly described|p1-11, p14|Mesoproterozoic|Mesoproterozoic|Contains 'string of beads' macrofossils, formally named in this article as Horodyskia williamsii and systematically described.||Of the Manganese Group||Overlies Whitewood Formation. Correlative of Backdoor Formation. Is overlain by Enachedong Dolomite.||
23987|Stag Arrow Formation|66948|5|Briefly described|p22, p23|||Intertidal environment. Contains H.williamsii.||Unit in Bangemall Supergroup.||||
23987|Stag Arrow Formation|67183|5|Briefly described|p643, 645, 647-9, 653, 661-3, 668, 671|Mesoproterozoic|Mesoproterozoic|Varies between 50 and 1500m thick. Now includes Bee Hill Sandstone.||Manganese Subgroup||Unconformably overlies Coondoon Formation, Carawine Dolomite and Pinjian Chert Breccia; conformably underlies Balfour Formation; suggested correlative of Waltha Woora Formation.|Well sorted sandstone locally interbedded with conglomerate, shale, chert and dolomite.|
23987|Stag Arrow Formation|67269|5|Briefly described|p20-21 Fig.19|||Bangemall Basin. Contains Conophyton new form stromatolites with an axial zone; photograph shown to demonstrate the continuity of such zones through geological time, and to support the biogenic origin of stromatolitic structures in Strelley Pool Formation (East Pilbara Terrane).||Collier Group.||||
23987|Stag Arrow Formation|68280|6|Mentioned|p26 fig 24|||Bangemall Basin.||Collier Group||||
23987|Stag Arrow Formation|70936|5|Briefly described|p61,72,74|Mesoproterozoic|Mesoproterozoic|Geological province: Pilbara Craton. Upper part contains enigmatic strings of beads macrofossils (Horodyskia williamsii; Grey et al., 2010) which have been identified at 49 localities over at least 500 km of strike length (Grey and Williams, 1990; Grey et al., 2002, 2010; Martin, 2004), representing an important biomarker not seen anywhere else in the Bangemall Supergroup stratigraphy.||Unit of Bangemall Supergroup.||||
23987|Stag Arrow Formation|71003|6|Mentioned|p61, p74|Mesoproterozoic|Mesoproterozoic|Pilbara Craton.||Manganese Group||||
23987|Stag Arrow Formation|71042|4|Described|p66 fig 2, p67-p69, p76, p79|Mesoproterozoic|Mesoproterozoic|Oakover Basin. Varies between 50 and 1500m in thickness||Manganese Group||Unconformably overlies the Carawine Dolomite, Pinjian Chert Breccia and the Coondoon Formations. Conformably overlain by the Balfour Formation. Overlain by the Enacheddong Dolomite.||28-MAY-19
23987|Stag Arrow Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||shale, conglomerate, crystalline dolostone/dolomite, sandstone|
81988|Star Trek Dolerite|72814|5|Briefly described|p201, Fig. 3, p202 Fig. 4, p204 Fig.6|||East of Zuleika Shear, Ora Banda Domain. Mineralised.||||Shown as intruding White Flag Formation.||
26148|Stark Bay Formation|14227|5|Briefly described|Enclos. 2|Miocene|Miocene|Presented as Stark Bay Fm.||||||07-FEB-11
26148|Stark Bay Formation|29693|6|Mentioned|Fig.7|||||||||
26148|Stark Bay Formation|31562|5|Briefly described|p13|||Latest Early Miocene & earliest Middle Miocene||||||
26148|Stark Bay Formation|32748|2|Defined|p28|middle Miocene|middle Miocene|Early Middle Miocene||||||
26148|Stark Bay Formation|34951|6|Mentioned|p114|||||||||
26148|Stark Bay Formation|36293|2|Defined|p201|middle Miocene|early Miocene|Early to Middle Miocene.E - M||||||
26148|Stark Bay Formation|38221|6|Mentioned|Fig.4|||Perth Basin||||||
26148|Stark Bay Formation|41751|6|Mentioned|p7|||||||||
26148|Stark Bay Formation|43805|6|Mentioned|p4|||||||||
26148|Stark Bay Formation|44144|4|Described|p502 Tb.4-21, p518 fig 4-162, p519|Middle Miocene|Early Miocene|Type Section: Gage Roads 2 well (362-577m).  230m thick marine shelf deposits.||||Overlies Kings Park Formation disconformably. Overlain by Wadjemup Formation unconformably.|Calcarenite, dolomite and chert.|
26148|Stark Bay Formation|61155|5|Briefly described|p15|Middle Miocene|Early Miocene|Age: 18-15.5Ma. Thickness: 200m. Geological Province: Perth Basin.||||||
26148|Stark Bay Formation|67925|6|Mentioned|Ch4 p8 fig 2|||||||Unconformably overlies the Kings Park Formation.||
23991|Steeple Peak Sandstone|13194|4|Described|p394 Tb. 4-16, p402 fig 4-66|Frasnian|Frasnian|Type Section: Steeple Peak 15o37'S 128o49'E. Zero to 260m thick tidal and fluvial deposits. Outcrops around Steeple Peak and Dillon Spring.||||Overlies Antrim Plateau Volcanics or Carlton Group (both unconformably). Laterally equivalent to Kellys Knob Sandstone.|Red quartz and feldspathic sandstone; rare conglomerate.|
23991|Steeple Peak Sandstone|40993|2|Defined|p4|Frasnian|Frasnian|Mention Fig.1||||||
23991|Steeple Peak Sandstone|41864|3|Fully described|p50|||In part previously assigned to Ragged Range Conglomerate.||||||15-DEC-08
23991|Steeple Peak Sandstone|41865|5|Briefly described|Map legend|Frasnian||||||||
23991|Steeple Peak Sandstone|42030|5|Briefly described|p749|||||||||
23991|Steeple Peak Sandstone|64580|6|Mentioned|map legend|||Of Cockatoo Group.||||||15-DEC-08
23991|Steeple Peak Sandstone|69165|6|Mentioned|500k_geologyp08_lut.csv|Frasnian|Frasnian|||Cockatoo Group||||
23991|Steeple Peak Sandstone|69452|6|Mentioned|p36:6|Frasnian|Frasnian|||Cockatoo Group.||||12-JUL-16
23991|Steeple Peak Sandstone|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Cockatoo Group.||||
23992|Steere Formation|23727|4|Described|p71|Proterozoic|Proterozoic|Of Mount Barren Group. Overlying unit Kundip Quartzite.||||||
23992|Steere Formation|23728|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Mount Barren Group. Overlying unit Kundip Quartzite. Geological Province Albany-Fraser Orogen.||||||
23992|Steere Formation|23752|4|Described|p13|Archean|Archean|Of Mount Barren Group. Overlying unit Kundip Quartzite.||||||07-NOV-08
23992|Steere Formation|23753|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mount Barren Group.  Dolomite; metamorphosed, massive to finely bedded; locally ?stromatolitic.  Geological Province: Albany-Fraser Orogen.||||||26-MAY-04
23992|Steere Formation|23754|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Mount Barren Group. Overlying unit Kundip Quartzite. Geological Province Albany-Fraser Orogen.||||||
23992|Steere Formation|42424|5|Briefly described|p4|||Reserved R. Thom 1980, listed as No Longer Required.||||||
23992|Steere Formation|44137|6|Mentioned|p257|||||Mount Barren Group.|||Quartzite, conglomerate and dolomite.|
23992|Steere Formation|62381|6|Mentioned|p4.|||||Basal unit in Mount Barren Group.||||
23992|Steere Formation|65487|4|Described|p22|Paleoproterozoic|Paleoproterozoic|Lowermost unit of the Mount Barren Group. Thin basal conglomerate overlain by pebbly sandstone and dolomitic limestone. Type locality: Western Steere River. Laterally discontinuous - may represent a restricted coastal depositional environment: fluvial or fluvial-deltaic. Overlies Manyutup Tonalite with a nonconformity or thrust contact.||||||10-FEB-14
23992|Steere Formation|67722|6|Mentioned|p8|Statherian|Statherian|||Mount Barren Group||||
23992|Steere Formation|68186|4|Described|p14|Paleoproterozoic|Paleoproterozoic|Type locality in the Western Steere River.||Basal Mount Barren Group.||Non-conformably overlies Manyutup Tonalite.|Thin basal conglomerate (clasts of quartzite, chert, BIF and felsic volcanic rocks), overlain by several metres of pebbly sandstone and 4m of dolomitic limestone.|
23992|Steere Formation|69252|5|Briefly described|p10-11|||Fluvial or fluvio-deltaic sediments.||Basal Mount Barren Group.||Nonconformably (?thrust fault) overlies Manyutup Tonalite. Overlies Kundip Quartzite.|Thin basal conglomerate with clasts of quartzite, chert, BIF and felsic volcanic rocks; overlain by several metres of bedded pebbly sandstone and four metres of dolomitic limestone.|
23992|Steere Formation|69595|4|Described|p8, p11 tbl 2, p11, p13 fig 7a, p15.|Orosirian|Orosirian|Yilgarn Craton, Barren Basin. Type locality in the Western Steere River. Deposited in a  fluvial-deltaic or shallow marine environment.  Approximately 12m thick. See also p36, p38, p58.|1990 +/- 16 Ma|Mount Barren Group||Non-conformably overlies the Manyutup Tonalite. Overlain by the Kundip Quartzite.|Thin basal conglomerate with clasts of quartzite, chert, banded-iron formation and felsic volcanic rocks that is overlain by several metres of pebbly sandstone and dolomitic limestone.|
23992|Steere Formation|70090|4|Described|p446,448,457-458|Statherian|Statherian|Geological province: Biranup Zone, Albany-Fraser Orogen, West Australian Craton; also Yilgarn Craton. Of Barren Basin. Thickness: ~12m. Depositional environment: Fluvial or fluvial-deltaic. Metamorphosed to greenschist facies. Similar detrital zircon pattern to Stirling Range Formation.||Unit of Mount Barren Group.||Lowermost unit of Mount Barren Group. Overlain by Kundip Quartzite. Underlain by Manyutup Tonalite.|Basal conglomerate overlain by pebbly sandstone and dolomitic limestone.|
26149|Stein Formation|22496|6|Mentioned|p11||Neoproterozoic|Kuniandi Group||||||
26149|Stein Formation|23806|5|Briefly described|p1123 Fig. 2|Neoproterozoic|Neoproterozoic|Of Kuniandi Group.||||||
26149|Stein Formation|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26149|Stein Formation|32660|5|Briefly described|Table 6|||||||||
26149|Stein Formation|32728|6|Mentioned|Table 7|||See also Fig.16||||||
26149|Stein Formation|36551|6|Mentioned|Table 10|||||||||
26149|Stein Formation|36888|4|Described|p215|||||||||
26149|Stein Formation|36898|5|Briefly described|Table III|||||||||
26149|Stein Formation|37927|5|Briefly described|p508|||||||||
26149|Stein Formation|38157|6|Mentioned|Table X|||||||||
26149|Stein Formation|41405|6|Mentioned|p206|||||||||
26149|Stein Formation|44140|5|Briefly described|p301 fig 4-7, p303 Tb.4-2|Neoproterozoic|Neoproterozoic|Of Mount Ramsay area. Up to 210 m thick.||Kuniandi Group||Overlies Landrigan Tillite conformably. Overlain by Wirara Formation conformably.|Purple ferruginous greywacke.|
26149|Stein Formation|44231|5|Briefly described|Map Legend|Neoproterozoic III|Neoproterozoic III|Of the Kuniandi Group. Purple, coarse-grained greywacke. Age: c.610Ma. Geological Province: Louisa Basin.||||||26-MAY-05
26149|Stein Formation|44397|14|Not recorded|p.15, Table 3||Adelaidean|Kuniandi Group. Defn. on Tech.File E/52-9.||||||
26149|Stein Formation|44398|14|Not recorded|map legend||Adelaidean|||||||
26149|Stein Formation|45047|4|Described|p36|||Kuniandi Group||||||
26149|Stein Formation|48927|2|Defined|p13|Adelaidean|Adelaidean|||||||
26149|Stein Formation|63458|6|Mentioned|p873 Fig.2, p881, p897 Fig.19.|Ediacaran|Ediacaran|||Unit in Kuniandi Group.||Overlies Landrigan Tillite.||
26149|Stein Formation|67484|6|Mentioned|p294 Tb.1|Ediacaran|Ediacaran|Mount Ramsay area, West Kimberley. ||Of the Kuniandi Group.||Overlain by the Wirara Formation. Underlain by the Landrigan Formation.||
26149|Stein Formation|67620|5|Briefly described|p5|Ediacaran|Ediacaran|Mount Ramsay area, Kimberley region.||Kuniandi Group.||Overlies Landrigan Formation. Is overlain by Wirara Formation.||
26149|Stein Formation|68138|6|Mentioned|p156|Neoproterozoic|Neoproterozoic|Mount Ramsay area, Kimberley region.||Kuniandi Group.||||
26149|Stein Formation|68244|4|Described|p660,664-666|Neoproterozoic|Neoproterozoic|Louisa Basin, Kimberley region.||Unit of Kuniandi Group.||Overlain by Wirara Formation. Underlain by Landrigan Formation.|Dark purple unit of interbedded sandstone and siltstone|
26149|Stein Formation|68473|6|Mentioned|p531|||Mount Ramsay.||Kuniandi Group||Equivalent to the Egan Formation.||
26149|Stein Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Kuniandi Group.|||Flaggy thinly bedded poorly sorted purple coarse greywacke with a ferruginous matrix and common graded bedding, cross bedding, slumps and ripples|
83116|Stennet granodiorite|71148|6|Mentioned|p134|||Appears in a Pb isotope ratios graph.||||||
83116|Stennet granodiorite|72485|6|Mentioned|p8 Fig.6, p12|||Norseman-Wiluna Belt. Informal name.  Illustrated as the crustal end-member of a mixing line for Pb isotope compositions.||||||04-APR-22
26911|Stockton Group|12758|5|Briefly described|p11|||Supersedes the Stockton Formation.  Geological Province: Collie Basin.||||||19-OCT-04
26911|Stockton Group|14227|5|Briefly described|p9, Enclos. 2|Early Permian|Early Permian|Includes Moorhead Formation overlying Shotts Formation. Underlies Westralia Sandstone. Glacial sediments. Geological Province: Collie Basin.||||||07-FEB-11
26911|Stockton Group|22818|5|Briefly described|map|Early Permian|Early Permian|||||||
26911|Stockton Group|22819|5|Briefly described|map|Early Permian|Early Permian|||||||
26911|Stockton Group|22820|4|Described|p8-9 Tbs. 1&2, p13, p24|Asselian|Tastubian|Supersedes Stockton Formation of Lord (1955). This group is extended here, by these authors to include Mosswood Formation with Moorhead and Shotts Formations. Geol. prov: Collie Basin. Glaciolacustrine/argillaceous sequence.||||||12-AUG-08
26911|Stockton Group|23174|5|Briefly described|Fig5p8|Early Permian|Early Permian|||||||
26911|Stockton Group|42711|5|Briefly described|p5 Fig. 4, p18-19, Plates 2, 4|Permian|Permian|Superseded Stockton Formation used by Lord (1952a) and Playford et al (1975) which has been replaced by Shotts Formation within the group. Comprises Shotts and Moorhead Formations. Geological province: Collie Basin. Nomenclatural history presented (p17)||||||11-AUG-08
26911|Stockton Group|61811|6|Mentioned|p35.|Permian|Permian|Southern Perth Basin. Continental deposits.||||||
26911|Stockton Group|64630|5|Briefly described|p31 Fig.2, p34|Sakmarian|Gzhelian|Province: Collie Subbasin. Underlies the Westralia Sandstone. Palynology age: D. tenuistriatus to P. confluens. Top correlates with the top of the Mosswood Formation. Constituents: Moorehead Formation and Shotts Formation.||||||12-SEP-13
26911|Stockton Group|64635|6|Mentioned|p18|Permian|Permian|Southern Perth Basin. Continental deposits.||||||
26911|Stockton Group|69182|6|Mentioned|Ch2 p9, Ch2 p45, Ch2 p47-p49|Early Permian|Early Permian|Perth Basin. See also Ch2 p55,Ch2 p57, Ch2 p60, Ch2 p64-p66, Ch2 p80, Ch2 p84, Ch2 p91, Ch2 p92, Ch2 p94-p96, Ch2 p98, Ch2 p100, Ch2 p102, Ch2 p104, Ch2 p106, Ch2 p108, Ch2 p110.|||Includes the Cullens Diamictite, Mosswood Formation and the Woodynook Sandstone.|Overlain by the Sue Group||
26911|Stockton Group|69297|6|Mentioned|p175, p189|Sakmarian|Asselian|Vlaming Sub-basin, South Perth Basin. |||Includes the Mosswood Formation.|||
26911|Stockton Group|70097|5|Briefly described|p19 Fig.3|Sakmarian|Asselian|Southern Perth Basin. Bunbury Trough and Collie Sub-basin.|||Mosswood, Moorhead, Shotts Formations.|||12-SEP-17
26911|Stockton Group|70099|5|Briefly described|Fig.4|Sakmarian|Asselian|Mentelle 1A Supersequence.|||Mosswood Formation.|Is overlain by Sue Group.||
26911|Stockton Group|70774|5|Briefly described|p5 fig 3|Sakmarian|Asselian|Collie Basin.|||Includes the Shotts Formation and the Moorehead Formation.|Overlain by the Westralia Sandstone.||
26911|Stockton Group|71377|5|Briefly described|p7|Permian|Carboniferous|Perth Basin.|||Includes the Mosswood Formation, Cullens Diamictite, Woodynook Sandstone, Rosabrook Coal Measures, Ashbrook Sandstone and the Redgate Coal Measures.|||
26911|Stockton Group|72034|5|Briefly described|500k_interpgeop16_lut|Sakmarian|Asselian|Carboniferous-Permian glacigene rocks, Perth Basin.  Age from biostratigraphy.|||||Diamictite overlain by claystone; lesser sandstone and siltstone.|
74807|Stockyard Basalt Member|64891|5|Briefly described|p39, p48-9 Tb. 1|Archean|Archean|Previously Stockyard Basalt of Watkins and Hickman (1990). Of the Meekatharra Formation. Overlain by Woolgra Andesite Member of Greensleeves Formation. Age: c.2780Ma. Geol.prov: Murch. Dom. Basalt and komatiitic basalt, minor felsic tuff; metamorphosed.||||||07-FEB-11
74807|Stockyard Basalt Member|67129|6|Mentioned|p18 Fig.19|Archean|Archean|Murchison Domain, Youanmi Terrane.||Meekatharra Formation.||||
74807|Stockyard Basalt Member|68110|5|Briefly described|p674 Fig. 2|Neoarchean|Neoarchean|Murchison Domain. Age constrained by that of the parent Meekatharra Formation.|c. 2792-2761 Ma|Of the Meekatharra Formation.||Conformably overlies Lordy Basalt Member.|Tholeiitic basalt.|09-OCT-14
74807|Stockyard Basalt Member|69583|5|Briefly described|p49|Neoarchean|Neoarchean|Murchison Domain.||Meekatharra Formation.||||
74807|Stockyard Basalt Member|69584|5|Briefly described|p5 Fig.2|Neoarchean|Neoarchean|||Meekatharra Formation||Overlies the Lordy Basalt|Komatiitic basalt.|
74807|Stockyard Basalt Member|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Meekatharra Formation.||||
74807|Stockyard Basalt Member|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv.|2800-2760 Ma|Unit of Meekatharra Formation.|||Basalt and komatiitic basalt, minor felsic tuff; metamorphosed|
74807|Stockyard Basalt Member|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.||Meekatharra Formation.|||Basalt and komatiitic basalt, minor felsic tuff; metamorphosed.|
74807|Stockyard Basalt Member|72389|5|Briefly described|Map Legend|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Gabanintha 1:100k map sheet 2644.||Meekatharra Formation|||Basalt and komatiitic basalt, minor felsic tuff; metamorphosed.|28-AUG-20
78697|Stockyard Gully Member|69788|3|Fully described|p1023-1024, p1029-1034, p1037|Pleistocene|Pleistocene|New name, from the Stockyard Gully cave system in the Eneabba region. 3-10m thick. Type locality is the exposed wall of the Beekeepers Doline. Capped by 20-40cm massive laminar calcrete. Has a loose or cemented reddish paleosol layer 1m thick on top.||Unit in Tamala Limestone.||Overlies Nambung Member. Is overlain by Pinnacles Desert Member and Cooloongup Sand.|Consists of an eolian calcarenite/calcrete-microbialite/paleosol cycle.|
78697|Stockyard Gully Member|69840|4|Described|p183, p187-8, p190 Fig.7, p190|Pleistocene|Pleistocene|See also p198 Fig.15, p199 Fig.16, p200, p196 Fig.13, p197. Date given: Marine Isotope Stage MIS 8-9.|c. 0.28 Ma|Tamala Limestone||Partially overlies Tamala Limestone and Nambung Member. Partially underlies Pinnacles Desert Member.|Aeolian calcarenite.|
68505|Stone Yard Granophyre|63441|2|Defined|p10 Tb. 2, p36|Archean|Archean|Of the Orpheus Supersuite. Age: 3014+/-6Ma. Geological province: Pilbara Craton. Intrudes Cleaverville Formation.||||||07-FEB-11
68505|Stone Yard Granophyre|64174|5|Briefly described|Map legend|Archean|Archean|Of the Orpheus Supersuite. Geological province: Pilbara Craton.  quartz-rich granophyre and quartz and feldspar-porphyritic dacite; metamorphosed.||||||07-NOV-08
68505|Stone Yard Granophyre|64580|4|Described|map legend||Mesoarchean|Of Orpheus Supersuite. Quartz-rich granophyre and quartz and feldspar porphyritic dacite; metamorphosed.||||||15-DEC-08
68505|Stone Yard Granophyre|67201|5|Briefly described|p16-17 Fig.9|Archean|Archean|Pilbara Craton. In Roebourne-Karratha area.||Orpheus Supersuite|||Quartz-rich granophyre and quartz and feldspar-porphyritic dacite; metamorphosed.|
68505|Stone Yard Granophyre|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Orpheus Supersuite.|||Quartz-rich granophyre and quartz and feldspar porphyritic dacite; metamorphosed|
68505|Stone Yard Granophyre|70775|5|Briefly described|p15, p47, p50|Mesoarchean|Mesoarchean|Pilbara Craton. This 2km long sill intrudes the Cleaverville Formation 500m north of Mount Ada. This unit hosts a c. 3100 Ma xenocrystic zircon from the underlying Whundo Group.|3014 +/- 6 Ma (Nelson, 1997j)|Orpheus Supersuite||Intrudes (locally) the Cleaverville Formation. Overlies the Whundo Group.|Quartz rich granophyre and quartz and feldspar-porphyritic dacite; metamorphosed.|
25494|Stoney Creek Conglomerate|24061|6|Mentioned|p175|||Geological Province:  Canning Basin.||||||
25494|Stoney Creek Conglomerate|41215|6|Mentioned|p277|||||||||
27574|Stony Creek Conglomerate|24503|5|Briefly described|Map legend|Devonian|Devonian|Boulder, cobble and pebble conglomerate.   Geological Province: Canning Basin.||||||
27574|Stony Creek Conglomerate|30525|6|Mentioned|Map legend|Devonian|Devonian|||||||
27574|Stony Creek Conglomerate|30533|4|Described|p24|||On Table 6||||||
27574|Stony Creek Conglomerate|31332|6|Mentioned|Fig. 3|||||||||
27574|Stony Creek Conglomerate|36890|4|Described|p335|||||||||
27574|Stony Creek Conglomerate|39796|6|Mentioned|Map legend|Devonian|Devonian|||||||
27574|Stony Creek Conglomerate|42030|6|Mentioned|p748|||||||||
27574|Stony Creek Conglomerate|42710|5|Briefly described|map legend|Late Devonian||||||||
27574|Stony Creek Conglomerate|42811|5|Briefly described|p43|||||||||
27574|Stony Creek Conglomerate|43281|6|Mentioned|Map legend|Late Devonian|Late Devonian|Canning Basin.||||||
27574|Stony Creek Conglomerate|44366|14|Not recorded|p.18, Table 3||Devonian|||||||
27574|Stony Creek Conglomerate|44367|14|Not recorded|map legend|||(Reprinted 1971).||||||
27574|Stony Creek Conglomerate|44403|2|Defined|p.11||Famennian|E/51-12. Famennian. Boulder to pebble conglomerate, greywacke and sandstone. Uncoformably U/lain by Pillara Formation.||||||
27574|Stony Creek Conglomerate|44404|14|Not recorded|map legend||Late Devonian|Upper Devonian.||||||
27574|Stony Creek Conglomerate|44998|14|Not recorded|p26, map|||(E51-8,12).||||||
27574|Stony Creek Conglomerate|45101|6|Mentioned|Fig.8|||||||||
27574|Stony Creek Conglomerate|45153|3|Fully described|App.3-52|||||||||
27574|Stony Creek Conglomerate|64580|6|Mentioned|map legend|||Frasnian and Famennian conglomerates associated with Devonian reef complexes.||||||15-DEC-08
27574|Stony Creek Conglomerate|66127|3|Fully described|pp142-143, p176, pp297-299, Plates 3, 7.|Late Frasnian|Middle Frasnian|Of Guppy et al. (1958); further described by Playford and Lowry (1966). Type locality specified in this study. Central Lennard Shelf. c.200 - 550 m thick sediments sourced from the Stony Creek Fault, active during the Devonian.||||Interfingers with Pillara Limestone and Virgin Hills Formation. Is overlain by Napier Formation.|Subrounded to well-rounded polymictic cobble and boulder conglomerate with lesser sandstone; granitic and quartzite clasts; fan-delta and submarine-fan deposits.|
27574|Stony Creek Conglomerate|69099|5|Briefly described|500k_geologyp08_lut.csv|Famennian|Frasnian|Frasnian and Famennian conglomerates associated with Devonian reef complexes.|||||Conglomerate and sandstone.|04-AUG-15
27574|Stony Creek Conglomerate|69165|6|Mentioned|500k_geologyp08_lut.csv|Famennian|Frasnian|||||||
27574|Stony Creek Conglomerate|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Massive boulder fanglomerate at the base overlain by mixed fluviatile to deltaic conglomerate and sandstone; clasts are rounded and mostly granitoid with lesser quartzite, vein quartz and foliated felsic volcanics|
27574|Stony Creek Conglomerate|71811|5|Briefly described|Map legend.|Frasnian|Frasnian|Canning Basin. A unit in the Devonian Reef Complexes: Frasnian platform and basin floor conglomerates associated with carbonate reef complexes.|||||Siliciclastic cobble to boulder conglomerate, minor sandstone and interbedded limestone.|06-MAY-19
79518|Stony Hill Dolerite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2680 Ma (inferred).|Great Boulder Suite|||Dolerite to basal pyroxenite; differentiated sill; metamorphosed.|
79518|Stony Hill Dolerite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2680 Ma (inferred)|Unit of Great Boulder Suite.|||Dolerite to basal pyroxenite; differentiated sill; metamorphosed|
40566|Stragglers Member|12758|5|Briefly described|p20-21, p10 Fig. 10|Early Cretaceous|Early Cretaceous|Of the Carnac Formation. Transitional with the Mangles Member above and the Jervoise Sandstone below. Thickness in type section: 191m. Geological Province: Vlaming Sub-basin.||||||28-JUL-09
40566|Stragglers Member|14227|5|Briefly described|Enclos. 2|Berriasian|Berriasian|Of Carnac Formation (Parmelia Group). Underlies Mangles Member. Presented as Stragglers.||||||07-FEB-11
40566|Stragglers Member|24443|5|Briefly described|Fig.31|Early Cretaceous|Late Jurassic|Of Carnac Formation. Conformably overlies Jervoise Sandstone. Conformably overlain by Mangles Member. Geological Province: Perth Basin.||||||
40566|Stragglers Member|50108|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Carnac Formation (Parmelia Group). Geological Province: Perth Basin.||||||28-JUL-09
40566|Stragglers Member|69182|6|Mentioned|Ch2 p15|Cretaceous|Cretaceous|Perth Basin.||Carnac Formation||||
40566|Stragglers Member|70097|5|Briefly described|p9|||Southern Perth Basin. Vlaming Sub-basin.||Carnac Formation||||
40566|Stragglers Member|71958|5|Briefly described|p14, p41, p45-p46|Early Cretaceous|Early Cretaceous|Vlaming Sub-basin. Contains sub-economic oil accumulations discovered in Gage Roads 1 and Gage Roads 2.||Carnac Formation||||
76820|Strawberry Rocks Monzogranite|68655|5|Briefly described|GEOCHRON 182711.1.pdf|Neoarchean|Neoarchean|Southern Cross Domain, Youanmi Terrane, Yilgarn Craton. SHRIMP U-Pb zircon age of magmatic crystallisation.|2680 +/- 4 Ma (Wingate et al., 2012).|||Abuts Widgiemooltha Dyke Suite.|Medium- to coarse-grained biotite metamonzogranite.|19-NOV-15
76820|Strawberry Rocks Monzogranite|69559|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|See also geologyp_lut.csv, 500k_interpgeop_lut.csv, Geochron report 182711.1.pdf.|2680+/-4 Ma U/Pb SHRIMP magmatic crystallisation||||Biotite monzogranite; fine to coarse grained; k-feldspar phyric.|
76820|Strawberry Rocks Monzogranite|70156|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma).Southern margin of the pluton coincides with E-trending dyke of Widgiemooltha Supersuite. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv. Sample GSWA 182711 (biotite metamonzogranite) yielded an interpreted magmatic crystallisation age of 2680+\4 Ma (weighted mean 207Pb*/206Pb*). Sample GSWA 199023 (biotite metamonzogranite) yielded an interpreted magmatic crystallisation age of 2681+\-3 Ma (concordia age).|2680+\-4 Ma (isotopic)||||Biotite monzogranite; medium to coarse grained; K-feldspar-phyric|
76820|Strawberry Rocks Monzogranite|70204|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton.|c.2680 Ma.||||Biotite monzogranite; fine- to coarse-grained; K-feldspar-phyric.|
76820|Strawberry Rocks Monzogranite|70794|5|Briefly described|500k_interpgeop_lut.csv|Neoarchean|Neoarchean|Also 100k_interpgeop_lut.csv, 100k_geologyp_lut.csv, 199023.1.pdf, 182711.1.pdf U/Pb SHRIMP data discussed.|2680+/-4 Ma||||Biotite monzogranite; medium-coarse grained; K-feldspar phyric.|
69696|Strelley Monzogranite|61253|5|Briefly described| p56|Archean|Archean|Age: 3.24Ga. Geological Province: Pilbara Craton.  Not related to Strelley Pool Chert.||||||07-NOV-08
69696|Strelley Monzogranite|63441|5|Briefly described|p9 Tb. 2|Archean|Archean|Of the Cleland Supersuite. Supersedes Strelley Granite. Ages: 3239+/-5Ma, 3239+/-2Ma and 3238+/-3ma. Geological province: Pilbara Craton.||||||07-FEB-11
69696|Strelley Monzogranite|63538|5|Briefly described|p5, p15, p16|Archaean|Archaean|Intrudes Sulphur Springs Group. K2O-rich subvolcanic laccolith. Geological Province: Pilbara Craton.||||||07-FEB-11
69696|Strelley Monzogranite|64580|4|Described|map legend||Paleoarchean|Of Cleland Supersuite. Hornblende-biotite monzogranite, granophyric monzogranite, and subvolcanic granitoid intrusions; metamorphosed.||||||15-DEC-08
69696|Strelley Monzogranite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Cleland Supersuite. 3239-3238 Ma. Hornblende-biotite monzogranite, granophyric monzogranite, and subvolcanic granitoid intrusions; metamorphosed.||||||
69696|Strelley Monzogranite|66217|5|Briefly described|p34.|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c.3240 Ma.|Unit in Cleland Supersuite.||||
69696|Strelley Monzogranite|67130|6|Mentioned|p16 |||This unit provided the heat which drove the formation of VMS Cu-Zn deposits.||||Intrudes Sulphur Springs Group|Rapakivi textured monzogranite|
69696|Strelley Monzogranite|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Mapped as 6 separate facies. See map legend for a detailed lithological description.||Of the Cleland Supersuite.|||Includes porphyritic hornblende-biotite monzogranite; equigranular hornblende-biotite monzogranite; layered monzogranite; fine-grained, granophyric monzogranite; microdiorite and diorite; dolerite and gabbro; all metamorphosed.|02-MAY-14
69696|Strelley Monzogranite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Cleland Supersuite|||Porphyritic hornblende--biotite monzogranite and granophyric monzogranite. Microdiorite, diorite, equigranular hornblende-biotite monzogranite, layered monzogranite, granophyric monzogranite, dolerite and gabbro.|
69696|Strelley Monzogranite|69185|4|Described|GEOL_LUT_CSV files||Paleoarchean|Geological Province: Pilbara Craton.|c. 3238 Ma|Unit of Cleland Supersuite.|||Hornblende-biotite monzogranite, granophyric monzogranite, and subvolcanic granitoid intrusions; metamorphosed|
69696|Strelley Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|3239-3238 Ma (isotopic, inferred)|Unit of Cleland Supersuite.|||Dolerite and gabbro, hornblende-biotite- monzogranite, layered and granophyric monzogranite, diorite and microdiorite.|
69696|Strelley Monzogranite|70775|6|Mentioned|p24-p25, p28|||Age is a Nd TDM date. May be related to the Sulphur Springs Group.|c. 3240 Ma|||||
69696|Strelley Monzogranite|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||monzogranite, granite|
69696|Strelley Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||Max age 3239+/-5 Ma, min 3238+/-3 Ma.|Cleland Supersuite|||Hornblende--biotite monzogranite and granophyric monzogranite; local diorite, dolerite, and gabbro; metamorphosed.|
69696|Strelley Monzogranite|72668|5|Briefly described|p9, p19, p27|||Atypical. Shows evidence for mingling between basaltic and felsic magmas, and a within-plate geochemical signature.|c.3200 Ma.||||Rapakivi-textured monzogranite.|14-JAN-22
74062|Strelley Pool Formation|64405|2|Defined|p1-22, p26 Appdx.|Archean|Archean|Supersedes Strelley Pool Chert. Max. thickness: 100m. Age: 3426-3350 Ma. Regarded as a regional stratigraphic marker between Warrawoona Group below (unconformable contact) and Euro Basalt (Kelly Group) above. Geol.prov: East Pilbara Terrane. Lith details.||||||08-SEP-14
74062|Strelley Pool Formation|64621|5|Briefly described|Map legend|Archean|Archean|Of the Pilbara Supergroup. Sandstone, conglomerate, chert, and silicified carbonate rocks; local silicified volcanic rocks; stromatolitic; metamorphosed.||||||07-NOV-08
74062|Strelley Pool Formation|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Unit in Pilbara Supergroup. Age: <3426 Ma. Silicified carbonate rocks, sandstone, conglomerate, chert, and dolomite; stromatolitic; metamorphosed.||||||16-APR-13
74062|Strelley Pool Formation|66118|5|Briefly described|p149, p150 Fig.4|||Pilbara Craton. East Pilbara Terrane. Thickness: 10-30 m.||At base of Kelly Group|||Silicifed stromatolitic carbonates with a local basal member of quartzite|
74062|Strelley Pool Formation|66122|6|Mentioned|p74|Archean|Archean|See also references to Strelley Pool Chert (p74-75, 84 Fig.6, p85-86).|3.42 - 3.35 Ga.|Warrawoona Group.||||
74062|Strelley Pool Formation|66217|4|Described|p1, p5, p6, p8, p10, p12, p17, pp28-29.|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Van Kranendonk et al. (2002) included this unit in the Salgash Subgroup in their redefinition of the Warrawoona Group. Revised by Hickman (2008) from Strelley Pool Chert of Lowe (1980, 1983) and Van Kranendonk and Morant (1998). Deposited across a regional subaerial erosional unconformity representing a 75 My hiatus in vulcanism. Detrital zircon age of 3426 +/- 10 Ma (Nelson 1998a) gives maximum depositional age.|c.3420-3350 Ma.|Unit in Pilbara Supergroup.||Overlies Salgash, Coongan and Talga Talga Subgroups unconformably. Is overlain conformably by Euro Basalt of the Kelly Group.|Basal unit of fluviatile to shallow-marine quartzite and conglomerate, overlain by a variably silicified unit of carbonate and stromatolitic carbonate, and an upper unit of coarse clastic sedimentary rocks deposited on receding alluvial fans.|
74062|Strelley Pool Formation|66664|5|Briefly described|p3, p6-8, p13 Fig.13.|Archean|Archean|East Pilbara Terrane. Diverse Archean stromatolite morphologies associated with sedimentary features protected within Trendall State Geoheritage Reserve.||Part of Pilbara Supergroup.|||Silicified carbonate and clastic sedimentary rocks.|05-SEP-14
74062|Strelley Pool Formation|66745|3|Fully described|pp50-59.|Paleoarchean|Paleoarchean|Distributed over 30,000 sq. kms. of a regionally peneplained surface. Author discusses reasons for not assigning this unit to Kelly Group, even though topmost part may be of similar age to Euro Basalt. Locally deep (many kilometres) subaerial erosion.|3426-3350 Ma.|Unit in Pilbara Supergroup.||Separates Warrawoona and Kelly Groups. Unconformably overlies Panorama Formation. Is paraconformably overlain by Euro Basalt.|Clastic sedimentary rocks, carbonate rocks, and chert; silicification of primary carbonate and fine-grained clastic rocks produced secondary 'chert'. Upper part contains conglomerate of clasts derived from lower part, and silicified volcanic ash.|
74062|Strelley Pool Formation|67130|5|Briefly described|p16, p23, p62, p75|Paleoarchean|Paleoarchean|Maximum thickness of 9.4 km. Also referred to as Strelley Pool Chert (p15 fig 10). East Pilbara Terrane. Stromatolites though to have been deposited under shallow marine, periodically evaporative conditions. See also p76, p79, p82 fig 81, p83 fig 82, p84 fig 84, p85 fig 85.|3350 Ma  |||Unconformably overlies Warrawoona Group,  Mount Ada Basalt, disconformably overlies Panorama Formation, conformably overlain by Euro Basalt|Fluviatile to shallow marine conglomerates, quartzite, stromatolitic marine carbonates and coarse clastic rocks.|
74062|Strelley Pool Formation|67197|3|Fully described|p1-64|Paleoarchean|Paleoarchean|Previously Strelley Pool Chert. Had been aassigned to basal Kelly Group. Type section (Lowe, 1983) is at Strelley Pool. Has a c.25 km strike length in the East Strelley greenstone belt of the East Pilbara Terrane, Pilbara Craton. A prominent stratigraphic marker horizon. Contains the world's oldest putative coniform stromatolites and putative biogenic microtubular structures. Metamorphosed to lower-greenschist facies. U-Pb zircon maximum age; minimum age from overlying Euro Basalt. Detailed discussion of lithologies, and biogenicity or otherwise of stromatolite structures. Many photomicrographs and photographs of outcrops.|3426-3350 Ma.|Pilbara Supergroup.||Unconformably overlies many units of the Warrawoona Group. Is overlain unconformably (?disconformably) by Euro Basalt (Kelly Group). Is faulted against Lalla Rookh Sandstone.|Five informal members are distinguished: basal sandstone and conglomerate; grey-white layered chert; stromatolite-bearing chert with crystal fans; upper chert; upper clastic rocks.|
74062|Strelley Pool Formation|67201|4|Described|p7 Fig.4, p10, p12 Tb.1|||In northern Pilbara Craton, East Pilbara Terrane. In Pilbara Supergroup the first break in volcanism (3425 - 3350 Ma), during which erosion of older uplifted and metamorphosed volcanic and granitic rocks accompanied by deposition of sedimentary rocks (Strelley Pool Formation), separated 3525-3427 Ma Warrawoona Group from 3350-3315 Ma Kelly Group. Age: between 3427-3350 Ma.|c. 3420 Ma|||Erosionally overlies Warrawoona Group (regional unconformity). Is disconformably overlain by Kelly Group.|Shallow water sedimentary rocks.|
74062|Strelley Pool Formation|67269|4|Described|p1-3, p6-27|Paleoarchean|Paleoarchean|Formerly Strelley Pool Chert, in the Warrawoona Group. Renamed the Strelley Pool Formation by Van Kranendonk et al. (2004, 2006) and moved into Kelly Group. Excluded from both Groups by Hickman (2008) due to absence of volcanic deposits. Crops out throughout many greenstone belts of the East Pilbara Terrane. Hosts the Trendall locality, a site containing a diverse assemblage of stromatolites and sedimentary facies. Putative microfossils have also been reported (Sugitani et al., 2010). Thickness generally between 20m and 100m; locally up to 1000m. Facies variations and stromatolites described in detail. Contains un-named stromatolites with an axial zone; photograph shown to demonstrate the continuity of such zones through geological time, and to support the biogenic origin of stromatolitic structures in this Formation.|3426-3350 Ma.|Pilbara Supergroup.||Unconformably to paraconformably overlies Panorama Formation (Warrawoona Group). Is overlain locally conformably by Euro Basalt (Kelly Group).|Silicified carbonate and clastic sedimentary rocks including basal conglomerate.|
74062|Strelley Pool Formation|67270|5|Briefly described|p2-4|Paleoarchean|Paleoarchean|East Pilbara Terrane.|<3426 Ma.|Pilbara Supergroup.||Unconformably overlies Panorama Formation (Warrawoona Group). Is overlain unconformably by Kelly Group.||
74062|Strelley Pool Formation|67668|5|Briefly described|Fig. 2-5; p. 154, 157, 159; Tb.1. ||Paleoarchean|East Pilbara Terrane, Pilbara Craton. Separates the Warrawoona and Kelly Groups. Marks a c.75 my pause in early Archean volcanic activity. Deposited in a largely shallow-water environment. Possible evidence of early life is reviewed. |ca 3427 - 3350 Ma.|||Underlies the Kelly Group, overlies the Warrawoona Group.|Consists of carbonates, sandstones and volcaniclastic sedimentary rocks; dominantly sandstone and chert.|
74062|Strelley Pool Formation|67888|6|Mentioned|p51|Archean|Archean||3426-3350 Ma|||||
74062|Strelley Pool Formation|68035|4|Described|p287, 293, p286 Fig 3, p288 Fig 4|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Shallow-water carbonate shelf sediments and stromatolites between the Warrawoona and Kelly groups. Up to 1 km thick. Age based on underlying and overlying units.|3426 - 3350 Ma|Of Pilbara Supergroup.||Unconformably overlies Panorama Formation, Salgash Subgroup, Warrawoona Group. Paraconformably overlain by Euro Basalt, Kelly Group.|Siliciclastic rocks, carbonate and chert.|
74062|Strelley Pool Formation|68280|5|Briefly described|p1, p3, p4, p5 , p6|Archean|Archean|Conglomerate within this unit is very coarse grained, with subrounded boulders up to 40cm in diameter. Blocks are composed primarily of chert and carbonate. Carbonate laminites are planar bedded. Radiating crystal fans occur in carbonate component of this unit. See also p13, p16, p19-p23, p29, p46. |<3426 Ma|||Unconformably overlies Mount Ada Basalt, disconformably overlies the Panorama Formation, overlain by Euro Basalt|Mafic volcanic rocks, siliciclastic rocks, sandstones, chert, chert pebble conglomerate and carbonate laminites with stromatolite fossils. Up to 30m Thick.|
74062|Strelley Pool Formation|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Detailed lithology discussed in map legend; the 4 facies are mapped separately.|< 3426 Ma|Of the Pilbara Supergroup.|||Felsic tuffaceous sandstone and quartz arenite; white, grey, and blue-black layered cherts, locally stromatolitic: either after dolomite or mainly silicified carbonate rocks; quartz-rich sandstone or arenite, thickly bedded; all metamorphosed.|23-SEP-13
74062|Strelley Pool Formation|68282|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. The 5 facies are mapped separately.|<3426 Ma|Of the Pilbara Supergroup|||Felsic volcaniclastic conglomerate and sandstone, minor felsic schist: locally silicified or carbonate cemented; hydrothermal chert in dykes; quartz-rich sandstone or arenite, thickly bedded; quartzite, weakly bedded.|
74062|Strelley Pool Formation|68283|5|Briefly described|Map Legend|Archean|Archean|East Pilbara Terrane, Pilbara Craton.||Of the Pilbara Supergroup.|||Silicified carbonate rocks, sandstone, conglomerate, chert, and dolomite; stromatolitic; metamorphosed.|23-SEP-13
74062|Strelley Pool Formation|68284|5|Briefly described|p1, 4-10, 20-22|Paleoarchean|Paleoarchean|Hickman (2008). Pilbara region. Formerly Strelley Pool Chert of Lowe (1983). Contains stromatolite-like structures (discussed in detail), a major feature of the Dawn of Life [geotourism] Trail. Up to 1000m thick locally. Shallow-marine and fluviatile environments. Photographs.|3426-3350 Ma (U-Pb; Hickman, 2008).|||Paraconformably to disconformably overlies Panorama Formation; locally overlies Mount Ada Basalt. Is overlain disconformably to paraconformably by Euro Basalt.|A succession of siliciclastic and volcaniclastic assemblages, laminated grey-white chert (from silicified carbonates), carbonate rocks with only minor silicification, and minor primary black, white, and jaspilitic chert with crystal fans.|
74062|Strelley Pool Formation|69012|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane. Four facies are mapped separately.|< 3426 Ma|Of the Pilbara Supergroup.|||Comprises silicified carbonate rocks, sandstone, conglomerate, chert, and dolomite; stromatolitic; metamorphosed.|29-APR-14
74062|Strelley Pool Formation|69013|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean||< 3426 Ma|Of the Pilbara Supergroup.|||Silicified carbonate rocks, sandstone, conglomerate, chert, and dolomite; stromatolitic; metamorphosed.|30-APR-14
74062|Strelley Pool Formation|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Includes 3 unnamed sub-units mapped separately. A quartz-rich sandstone or arenite unit near the base of this unit was dated at < 3426 Ma.||Of the Pilbara Supergroup.|||Silicified carbonate rocks, sandstone, conglomerate, chert, and dolomite, stromatolitic; layered chert after dolomite; quartz-rich sandstone or arenite; felsic volcaniclastic conglomerate and sandstone, minor felsic schist; all metamorphosed.|02-MAY-14
74062|Strelley Pool Formation|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Minor felsic schist, felsic tuffaceous sandstone.||Pilbara Supergroup|||Silicified carbonate rocks, sandstone, conglomerate, chert, and dolomite; stromatolitic; metamorphosed. Quartzite, quartz rich sandstone or arenite, hydrothermal chert, layered chert, felsic volcaniclastic conglomerate and sandstone.|
74062|Strelley Pool Formation|69301|4|Described|p5 Fig.3, p9 Tb.1, p10-11, p19-20, p23|||Pilbara Craton. East Pilbara Terrane. Buick et al. (1995) recognized and documented Earth's oldest erosional unconformity underlying the 3.43 Ga Strelley Pool Formation. |3420 Ma; 3.43 Ga|Pilbara Supergroup||Paraconformity at top. Is disconformably overlain by Kelly Group. (Regional) unconformity at base. Overlies Warrawoona Group.|Siliciclastic rocks, carbonates, banded-iron formation. Shallow-water marine to subaerial sedimentary rocks contain a diverse range of stromatolites, and microbial mats (due to prolonged break in volcanism).|
74062|Strelley Pool Formation|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Contains boulders of jaspilitic banded iron-formation at the base of the formation, likely derived from the Panorama Formation or Mount Ada Basalt or Duffer Formation. Sample GSWA 178043 (lithic-quartz sandstone) yielded an intepreted maximum depositional age of 3502+\-3 Ma for the sandstone. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv.|3426-3350 Ma (isotopic, inferred)|Unit of Pilbara Supergroup.||Underlain by Panorama Formation.|Felsic volcaniclastic conglomerate and sandstone and tuffaceous sandstone, layered chert, quartzite and quartz-rich sandstone and arenite, silicified carbonate rocks and felsic volcaniclastics.|
74062|Strelley Pool Formation|70022|5|Briefly described|p113, 115-119|||East Pilbara Terrane. Has a cluster of zircons aged 3,602 +/- 5 Ma.|3.43 - 3.35 Ga.|Pilbara Supergroup.||Unconformably overlies Warrawoona Group. Is overlain by Kelly Group.|Volcaniclastic sandstone.|
74062|Strelley Pool Formation|70507|5|Briefly described|p431,442-443,446-447|Paleoarchean|Paleoarchean|Geological province: Pilbara Craton. Contains photoautotrophic stromatolites (Allwood et al., 2007).|~3.4 Ga|Unit of Kelly Group.||||
74062|Strelley Pool Formation|70729|6|Mentioned|p164|||Geological province: East Pilbara Terrane, Pilbara Craton.||||||
74062|Strelley Pool Formation|70775|5|Briefly described|p12|Paleoarchean|Paleoarchean|East Pilbara.|c. 3420 Ma|Pilbara Supergroup||Unconformably overlies the Warrawoona Group. Disconformably overlain by the Kelly Group.||
74062|Strelley Pool Formation|70834|6|Mentioned|p298|Paleoarchean|Paleoarchean|Marble Bar greenstone belt, Pilbara Craton.||||Unconformably overlies Panorama Formation. Is overlain by Euro Basalt.|Siliciclastics, chert.|
74062|Strelley Pool Formation|70884|5|Briefly described|p123-126,128-131,133-137|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Thickness: up to 1km. Basin infill during erosion/non-deposition of the uppermost Warrawoona Group, providing evidence for sub-aerial weathering. Silicification observed within felsic rocks in shear zones in the Low-Strain belt.|<3.45 Ga|Unit of Pilbara Supergroup.||Overlain paraconformably by Euro Basalt/Kelly Group. Underlain unconformably by Warrawoona Group/Salagah Subgroup.|Quartz-sandstone.|
74062|Strelley Pool Formation|71136|6|Mentioned|p268|||Photomicrographs of microfossils used for comparison with those suggested in the Farrel Quartzite.||||||
74062|Strelley Pool Formation|71137|6|Mentioned|p14-15|Archean|Archean|Lowe (1983). Microfossils compared with those in Farrel Quartzite. See also reference to Strelley Pool Chert (p4).|3.4 Ga.|||||
74062|Strelley Pool Formation|71267|6|Mentioned|1m_geologyl12_lithology_lut.csv||||||||chert, limestone, sandstone, volcaniclastic rock|
74062|Strelley Pool Formation|71487|4|Described|p125,127-133,135-136|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Abbreviated as SPF in text. Prominent regional stratigraphic marker recognized in 11 of 20 greenstone belts throughout the East Pilbara Terrane. Deposited in a volcanically quiescent period of up to 75my. Upper part of the stratigraphy comprises recycled breccias and conglomerates from the lower part, indicating multiple periods of erosion prior to Euro Basalt deposition (Hickman, 2008). Hosts variably silicified dolomitic stromatolites comprising spectacular macroscopic evidence for early life on Earth (Hofmann et al., 1999; Allwood et al., 2007). Experienced lower- to sub-greenschist facies regional metamorphism. Cut by anastomosing, hydrothermal veins comprising primarily of fine-grained quartz (chert) across and parallel to bedding. Detailed petrography and D18O analysis of quarts/chert veins reveal a Paleoarchean hydrothermal event and a more recent, post-Archean event that resulted in the development of the hydrothermal quartz/chert veining in teh Strelley Pool Formation.|c. 3.4 Ga|Unit of Pilbara Supergroup.||Overlain conformably by Euro Basalt. Underlain unconformably by Warrawoona Group.|Basal to medium-grained sandstone and pebble to boulder conglomerate, bedded dolomite, (variably siliciflied) stromatolitic dolomite, and upper cobble to boulder conglomerates, coarse sandstones, and breccia.|
74062|Strelley Pool Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Pilbara Supergroup|||Silicified carbonate rocks, sandstone, conglomerate, chert, and dolomite; stromatolitic; metamorphosed.|
74062|Strelley Pool Formation|72064|4|Described|p64-67,76-81|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Thickness at type locality (21 06¿40.2¿ S, 119 08¿24.2¿ E): ~25m. Average thickness varies from between 10 metres to almost one km. Deposited within a shallow-water environment above an erosional unconformity upon a continental shelf (Hickman, 2008). Key sedimentary marker horizon within the dominantly volcanic Pilbara Supergroup. U-Pb study of detrital zircons by Nelson (1998) yielded youngest maximum depositional age of 3426+\-10 Ma in Warralong Greenstone Belt. Contains detrital zircons with ages c. 3479+\-10 Ma. U-Pb geochronology from this study yields two main zircon age populations at 3533-3409 Ma and 3645-3562 Ma. Based on this study, assigned maximum depositional age for the base of the SPF of 3414+\-34 Ma, above older continental crust that had already partially stabilized and emerged above sea-level, upon a shallow-water sedimentary platform (DiMarco and Lowe, 1989; Hickman, 2008; Van Kranendonk et al., 2006, 2003). Localised uplift and erosion of older Pilbara Supergroup units, and deposition of clastic detritus onto SPF.|3414 +/- 34 Ma (SHRIMP U-Pb, Max dep)|Unit of Pilbara Supergroup.||Overlain paraconformably by Kelly Group/Euro Basalt. Underlain by Warrawoona Group and the Panorama Formation. Unconformably overlies the Double Bar Formation.|Silicified sandstone, carbonate, chert, and volcaniclastic sediments.|28-JAN-20
74062|Strelley Pool Formation|72251|5|Briefly described|p54|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Pilbara Supergroup.||Overlain by Euro Basalt. Underlain by Warrawoona Group.||
74062|Strelley Pool Formation|72487|5|Briefly described|p1-2, 5, 10|Archean|Archean|East Pilbara Terrane, Pilbara Craton. Typically 8-11m thick; occurs over at least 30,000 km2. Microfossils include filaments, films, spheroids and lenses: their biogenic origins are discussed in detail.|3.46 Ga.||||Sandstones, shales, carbonates (mainly bedded and stromatolitic dolomite), chert units, and volcaniclastic rocks. Deposition in shallow-water. Carbonaceous cherts contains abundant microfossils.|
74062|Strelley Pool Formation|73598|6|Mentioned|p1212-12213|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Pilbara Supergroup.||Unconformably overlies Panorama Formation (Salgash Subgroup) and Warrawoona Group. Is overlain by Euro Basalt (Kelly Group).||
32783|Strutton Intrusion|44229|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
32783|Strutton Intrusion|60429|2|Defined|p13, p36 Appdx. 1|Archean|Archean|Mafic,discordant body of metagabbro+ minor metapyroxenite + serpentinized peridotite at base. Discordantly intrudes/cuts obliquely across Duffer Formation+overlying Apex Basalt. Intruded by Coppin Gap Granodiorite.Age: c.3471-c.3314Ma. Max.thickne:~500m.||||||07-FEB-11
32783|Strutton Intrusion|64936|5|Briefly described|map legend|Archean|Archean|Metagabbro and metapyroxinite. Shown associated with Kelly Subgroup units. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
32783|Strutton Intrusion|66217|5|Briefly described|p34|Paleoarchean|Paleoarchean|May be related to/contemporaneous with Gap Intrusion. Interpreted to represent subvolcanic intrusions to the Euro Basalt.||||Underlies Gap Intrusion in some areas, but has screen of greenstone between, in other areas.|Thick sill of gabbro, pyroxenite, and peridotite.|
32783|Strutton Intrusion|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Emu Pool Supersuite.|||Metagabbro and metapyroxenite.|06-JAN-15
32783|Strutton Intrusion|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Warrawoona Group|||Gabbro, pyroxenite, and peridotite; metamorphosed|
32783|Strutton Intrusion|69185|5|Briefly described|GEOL_LUT_CSV files||Archean|Geological province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_interpgeop_pilcrat02_lut.csv, 500k_interpgeol_pilcrat02_lut.csv.||||||
32783|Strutton Intrusion|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||gabbro, pyroxenite, serpentinite|
32783|Strutton Intrusion|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Warrawoona  Large Igneous Province.||Warrawoona Group|||Gabbro, pyroxenite, and peridotite; metamorphosed.|
74592|Stubbins Formation|63866|5|Briefly described|p92, p99|||Tanami Region.||||||
74592|Stubbins Formation|64277|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: c. 1864Ma. Feldspathic wacke, sandstone, siltstone, mudstone, dolerite and gabbro sills; minor quartzite, banded chert, and basalt, metamorphosed.||||||07-NOV-08
74592|Stubbins Formation|64722|5|Briefly described|Fig. 2 p3-6, p10, 24|Orosirian|Orosirian|Forms the base of the Paleoproterozoic succession in the Tanami Region. Interpreted as backarc basin deposits.|~1864 Ma.|||Unconformably overlain by Tanami Group.|Deep water sedimentary rocks and intercalated mafic rocks and dolerite sills.|11-APR-12
74592|Stubbins Formation|64730|5|Briefly described|p141-142|Orosirian|Orosirian|Ages from intrusive quartz porphyry.|Depositional age: max. ~1865 Ma, min. 1864+/-3 Ma.|||Unconformably underlies Tanami Group.|Sedimentary rocks.|03-MAY-12
74592|Stubbins Formation|64733|3|Fully described|p168-182, Figs.2, 4-12, Tab.1|Orosirian|Orosirian|Previously informally named Bald Hill Succession Bagas and Huston (2005). Previously thought to be part of Killi Killi Formation. Lithologically similar to Dead Bullock Formation, but older. Eastern contact is in faulted contact with Killi Killi Formation. Deposited in a back-arc to volcanic arc setting in a subaqueous environment.|Dated at 1864 +/- 3 Ma.|||Underlies Tanami Group.|Turbiditic sandstone, pelite, chert, dolerite sills, and rare basalt.|20-APR-12
74592|Stubbins Formation|64734|5|Briefly described|p187|Orosirian||In western Tanami region; coarse stacking turbiditic sequence; geochronological data indicates younger than Billabong Complex; Max. depositional age ~1865 Ma; min. age from rhyodacite within this unit ca. 1864 Ma; likely the basal known unit in the region||||||10-FEB-11
74592|Stubbins Formation|64735|6|Mentioned|p216 Fig15, p217,|||Tanami region. Possibly correlates with Warramunga Formation.||||||30-APR-12
74592|Stubbins Formation|64737|5|Briefly described|p232, p232 Fig.2||Orosirian||~1860 Ma.|||Underlies Tanami Group.||01-MAY-12
74592|Stubbins Formation|66129|5|Briefly described|p213, p214 Fig.1, p215 Fig.2, p216 Fig.3|Orosirian|Orosirian|1864 Ma. Turbiditic sandstone, siltstone, shale, dolerite and gabbro sills, banded chert, basalt; contact metamorphosed.||||||
74592|Stubbins Formation|66468|5|Briefly described|p16-17,p19-20, p21 Fig.6, p22-24,p26-27|Orosirian|Orosirian|1864 +/- 4 Ma. 2-3 km thick. Sandstone, siltstone, Fe-rich shale, chert and volcanic rocks. Conformably overlain by Killi Killi Formation. Hosts gold occurrence. High density and magnetic susceptibility due to abundant mafic rocks.||||||
74592|Stubbins Formation|67323|5|Briefly described|p29|||Granites-Tanami terrane. Continental back-arc setting.|1865 Ma.|||Is overlain unconformably by the lower Tanami Group.|Sandstone, siltstone, mudstone and basalt.|
74592|Stubbins Formation|67824|4|Described|p385 Fig.2, p386 Fig.3, p387 |Orosirian|Orosirian|Oldest known Paleoproterozoic rocks in the Tanami region. Age from detrital zircon and cross-cutting quartz-porphyry rhyodacite.|1864 +/- 4 Ma.|||Conformably overlain by the Killi Killi Formation.|A succession of banded iron formation, shale, chert, basalt, dolerite sills and rhyodacite.|
74592|Stubbins Formation|67826|4|Described|p400, p401 Fig.2, p402, p404 Fig.4, p406|Orosirian|Orosirian|Oldest recognised Paleoproterozoic unit in the Tanami region. Hosts several gold deposits and prospects (including the Sandpiper deposit and the Kookaburra deposit). Gold mineralisation dated to 1794 +/- 12 Ma (ore-related sericite). Age determined using 207Pb/206Pb zircon dating of a rhyodacite in this Formation.|~ 1864 +/- 4 Ma|||Overlain by the Killi Killi Formation; layer-parallel fault contact.|Consists of iron-rich siltstone, metamorphosed BIF, graphitic claystone, chert, turbiditic sedimentary rocks, basalt and dolerite sills.|
74592|Stubbins Formation|68474|4|Described|p570, p572-580, p584-585|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen. Constituent lithologies have similar geochemistry suggesting a genetic relationship. Occurs in the Bald Hill area of the GTO and at depth in the Coyote gold mine. 2-3km thick succession of turbiditic and low energy sedimentary rocks interbedded with volcanics and sills. Shares similarities with the Dead Bullock Formation the Mount Charles Formation. Geochemistry discussed in detail. Back arc basin affinity.|ca 1864 +/- 3 Ma (igneous crystallisation)|Tanami Group||Conformably overlain by the Killi Killi Formation.|Pillow basalt and dolerite sills with tholeiitic affinity.|
74592|Stubbins Formation|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. See also 500k_intergeop_lut.csv|c.1864 Ma (Bagas et al., 2008).|||Is intruded by Balwina Granite.|Feldspathic wacke, sandstone, siltstone, mudstone, and dolerite and gabbro sills; minor quartzite, banded chert, and basalt; metamorphosed|
74592|Stubbins Formation|69003|4|Described|p17|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. Deformed by the c.1844-c.1825 Ma Tanami Event and the c.1795 Ma Tanami Orogeny.|1864 +/- 4 Ma (Crispe et al., 2007).|Tanami Group.||Is overlain unconformably by Killi Killi Formation. Lateral equivalent of Dead Bullock and Mount Charles Formations.|Turbidites, basaltic rocks, and felsic volcanic rocks.|
74592|Stubbins Formation|69253|5|Briefly described|p746, p755|Orosirian|Orosirian|In WA, now included in the enlarged Dead Bullock Formation (Bagas et al., 2008, 2009, 2010, 2013).||||||
74592|Stubbins Formation|69426|5|Briefly described|p11:3-5|Orosirian|Orosirian|2000-3000m thick. Turbiditic to quiet marine conditions. SHRIMP U-Pb zircon igneous (rhyolite) crystallisation age; oldest known unit in the Group. Not mapped in the NT.|1864 +/- 3 Ma (Bagas et al., 2009).|Tanami Group.|Bald Hill Member.||Sandstone, siltstone, shale in lower part overlain by iron-rich siltstone, carbonaceous shale, chert, pillow basalt, dolerite sills, rare rhyolite.|12-JUL-16
74592|Stubbins Formation|69577|6|Mentioned|p117 Fig.6|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||||||
74592|Stubbins Formation|69587|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Geological province: Granites-Tanami Orogen, North Australian Craton. Events: Alice Springs Orogeny; Tanami Orogeny D1t. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeol_lut.csv.|1864 Ma (inferred; isotopic)|||Intruded by Balwina Granite.|Metamorphosed feldspathic wacke, sandstone, siltstone, mudstone, and dolerite; contact-metamorphosed, and metadolerite and gabbro sills; minor quartzite, metamorphosed banded chert, and metabasalt|
74592|Stubbins Formation|69618|5|Briefly described|p89-95, p97-98, p100 Tb.1, p106|Paleoproterozoic|Paleoproterozoic|Bagas et al. (2008). Here included in Madigan Beds of Dead Bullock Formation: reasons explained.|1864 +/- 4 Ma.|Unit in Tanami Group.||Is overlain transitionally by Killi Killi Formation.|Turbiditic sandstone, shale, interstratified pillow basalt; common dolerite sills; local ferruginous shale and BIF; rare rhyolite and banded and nodular chert towards the top of the sequence.|
74592|Stubbins Formation|69747|5|Briefly described|p262,264,268-271,274|||Geological province: Tanami Block, North Australian Craton. Intruded by dolerite sills (e.g. Coora, Groundrush) that have been metamorphosed to upper greenschist to amphibolite facies. Contain mafic suites that show similar geochemical characteristics to enriched back-arc basin basalt. Part of the transitional zone between Dead Bullock Formation and Killi Killi Formation. Nomenclature is superseded, replaced by Dead Bullock Formation.||||||
74592|Stubbins Formation|70129|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. Two facies associations are also mapped separately; biotite zone contact-metamorphosed psammite and pelite and metadolerite; and a metamorphosed dolerite sill with minor interlayered metamorphosed feldspathic wacke, sandstone, siltstone and mudstone (section only).|c.1864 Ma (Bagas et al., 2008).||||Metamorphosed feldspathic wacke, sandstone, siltstone, mudstone, and dolerite and gabbro sills; minor quartzite, metamorphosed banded chert, and metabasalt.|13-NOV-15
74592|Stubbins Formation|70130|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|c.1864 Ma (Bagas et al., 2008).|Tanami Group.|||Metamorphosed feldspathic wacke, sandstone, siltstone, mudstone, and dolerite and gabbro sills; minor quartzite, metamorphosed banded chert, and metabasalt.|
74592|Stubbins Formation|70141|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|c.1864 Ma.|||Is overlain by Killi Killi Formation.|Metamorphosed feldspathic wacke, sandstone, siltstone, mudstone, and dolerite and gabbro sills; minor quartzite, metamorphosed banded chert and metabasalt. Contact metamorphosed (biotite zone) psammite and pelite, and metadolerite, separately mapped.|
74592|Stubbins Formation|70142|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. Three sub-units are mapped separately: biotite-zone contact metamorphosed metadolerite; biotite-zone contact metamorphosed psammite and pelite, and metadolerite; metadolerite sill and minor interlayered, metamorphosed feldspathic wacke, sandstone, siltstone and mudstone.|c.1864 Ma.|||Is overlain by Tanami Group.|Metamorphosed feldspathic wacke, sandstone, siltstone, mudstone, and dolerite and gabbro sills; minor quartzite, metamorphosed banded chert, and metabasalt.|
74592|Stubbins Formation|70143|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. The four facies are mapped separately.|c.1864 Ma.||||Metamorphosed feldspathic wacke, sandstone, siltstone, mudstone and dolerite and gabbro sills, minor quartzite, metamorphosed banded chert, and metabasalt. Metadolerite sill. Contact-metamorphosed: metadolerite; psammite and pelite, and metadolerite.|
74592|Stubbins Formation|70154|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic||1864 Ma||||Metamorphosed feldspathic wacke, sandstone, siltstone, mudstone, and dolerite and gabbro sills; minor quartzite, metamorphosed banded chert, and metabasalt|
74592|Stubbins Formation|71267|5|Briefly described|500k_interpgeop16_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Granites-Tanami Orogen. Events: Alice Springs Orogeny (450-295 Ma); Stafford Event (1810-1790 Ma); Tanami Event (1850-1830 Ma).|1864+\-4 Ma (isotopic)|Unit of Tanami Group.|||Metamorphosed feldspathic wacke, sandstone, siltstone, mudstone, and dolerite and gabbro sills; minor quartzite, metamorphosed banded chert, and metabasalt|
74592|Stubbins Formation|71397|4|Described|p5,22,46-47|Orosirian|Orosirian|Geological province: Granites-Tanami Orogen. Cross and Crispe (2007) provided a depositional date of 1864+\-3 Ma (rhyolitic porphyry); maximum depositional ages reported as c. 1875 Ma and  c. 1869 Ma (Maidment et al., written comm., 2016). Deposition is broadly coeval with extension and emplacement of 1864-1852 Ma Paperbark Supersuite in the Western Zone; Tickalara Metamorphics sedimentaru protolith deposition in the Central Zone, and deposition of Biscay and Olympio formations in Eastern Zone.|c. 1864 Ma|Unit of Tanami Group.||Coeval with Paperbark Supersuite, Biscay Formation and Olympio Formation.|Sandstone and siltstone turbiditic rocks overlain by ferruginous and carbonaceous fine-grained lithofacies with intercalated basalt and dolerite.|
74592|Stubbins Formation|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1864+/-3 Ma (MDA: U-Pb zircon SHRIMP)||||Greywacke.|
74592|Stubbins Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. Includes informal 'metadolerite' subunit.|1864+/-4 Ma|Tanami Group|||Metamorphosed feldspathic wacke, sandstone, siltstone, mudstone, and dolerite and gabbro sills; minor quartzite, metamorphosed banded chert, and metabasalt.|
74592|Stubbins Formation|73089|4|Described|p: 1, 3, 5-7, ~11-19, ~22-29, 37, 41, 43|Orosirian|Orosirian|2-3 km thick. Low energy marine depositional setting; turbidity currents. Bagas et al. (2008) suggested it was stratigraphically below Dead Bullock Formation based on differences in geochemistry; however, Bagas et al. (2014) suggested that the two are lithologically similar, thus correlative. Stratigraphic position may be a correlative of a transitional zone between the Dead Bullock and Killi Killi formations. [Transitional contact with the overlying Killi Killi Formation?]. Upper portion is dominantly Paleoproterozoic detritus. Geochron sample numbers for metasandstones from: Kookaburra prospect = GSWA 177279, Sandpiper prospect = GSWA 178809 [see report for geochon details]. [A fine-grained felsic igneous rock in this unit was also dated but not explicitly attributed to the unit]. Includes an unpublished date of 1864 +/- 3 Ma for a felsic rock interpreted as a rhyolite within this unit (Bagas et al., 2008). Possibly broadly correlative to Biscay Formation. Geochemical characteristics of mafic extrusive and intrusive rocks within the unit suggests a back-arc setting.|1885-1865 Ma|||Correlates to Dead Bullock Formation. Intruded by Lewis Granite.|Lower succession of sandstone, siltstone, shale, rare rhyolite; upper package of Fe-rich siltstone and shale, graphitic and carbonaceous shale, chert, basalt, rare turbiditic sandstone.|
74592|Stubbins Formation|73158|6|Mentioned|p3, p10|||Restricted to Western Australia, suggested equivalent of Dead Bullock Formation.||||||
74592|Stubbins Formation|73159|5|Briefly described|p3, 10|||Granites-Tanami Orogen (Western Australian only). HFSE geochemical plots.||Tanami Group.||?Equivalent to Dead Bullock Formation.||
80981|Stubbins Formation - metadolerite 80981|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen||Stubbins Formation|||Metamorphosed dolerite sill; minor interlayered, metamorphosed feldspathic wacke, sandstone, siltstone, and mudstone.|
81578|Subchamber-D intrusion|71873|5|Briefly described|p427-428,433-434,436-438,440-441,444|Orosirian|Orosirian|Geological province: Lamboo Province. U-Pb detrital zircon magmatic age include 1844+\-3 Ma.||Unit of Sally Malay Complex.|||Weakly-layered orthocumulate hornblende gabbronorites to hornblende olivine gabbronorites with abundant large hornblende oikocrysts.|
34554|Sue Group|12758|5|Briefly described|p13, p3 Fig. 3, p9|Late Permian - Correct|Early Permian|Supersedes Sue Coal Measures. Comprises  Woodynook Sst., Rosabrook C.M., Ashbrook Sst., Redgate C.M. and Willespie Fm.  Overlain by Sabina Sst; conformably underlain by Mosswood Fm.  Geological Province: Southern Perth Basin.  See also p8 Fig. 9, p57.||||||13-DEC-07
34554|Sue Group|14227|5|Briefly described|p12, Enclos. 2|Dorashamian|Sakmarian|Includes: Willespie Formation; Redgate, Ashbrook and Rosabrook Coal Measures; and Woodynook Sandstone. Overlies Mosswood Formation. Gas occurs in its tight sands. Geol. Prov: Bunbury Trough, southern Perth Basin.||||||07-FEB-11
34554|Sue Group|22818|5|Briefly described|map|Late Permian|Early Permian|||||||
34554|Sue Group|22819|5|Briefly described|map|Late Permian|Early Permian|||||||
34554|Sue Group|22820|3|Fully described|p8-9 Tbs. 1&2, p15|Late Permian|Early Permian|Includes Woodynook Sst, Rosabrook CM, Ashbrook Sst, Redgate CM, Willespie Fm. Conformable on Stockton Gp; unconform.under Warnbro Gp. Thickness: ~1700m. Coal-bearing  siliciclastic rocks with sandstone dominating, and conglomerate/siltstone/mudstone/coal.||||||23-JUL-15
34554|Sue Group|24246|5|Briefly described|p6|Permian|Permian|Geological Province: Perth Basin.||||||
34554|Sue Group|24443|5|Briefly described|Fig.31|Late Permian|Early Permian|Conformably overlies Mosswood Formation. Conformably overlain by Sabina Sandstone. Geological Province: Perth Basin.||||||
34554|Sue Group|50107|5|Briefly described|Map legend|Permian|Permian|Geological Province: Southern Perth Basin.||||||
34554|Sue Group|61811|6|Mentioned|p35.|Permian|Permian|Southern Perth Basin. Continental deposits.||||||
34554|Sue Group|64635|6|Mentioned|p18|Permian|Permian|Southern Perth Basin. Continental deposits.||||||
34554|Sue Group|67925|4|Described|ES p6,Ch2 p2, Ch2 p5-p6, Ch2 p10 fig 4, |Changhsingian|Sakmarian|Replaces the older Sue Coal Measures. See also Ch2 p20, Ch2 p26-p27, Ch3 p6, Ch3 p8, Ch3 p15, Ch4 p5, Ch4 p9-p11, Ch4 p13-p14, Ch4 p30 fig 34, Ch5 p12-p13, Ch5 p17, Ch5 p20-p21, Ch5 p23-p24, Ch5 p26, Ch5 p28, Ch5 p32, Ch5 p36-p40, Ch6 p11, Ch6 p13, Ch7 p39, Ch8 p6-p7.|||Includes the Woodynook Sandstone, Rosabrook Coal Measures, Ashbrook Sandstone, Redgate Coal Measures, Willespie Formation|Overlies the Mosswood Formation. Overlain by the Sabina Sandstone.|Interbedded sandstone, siltstone, shale and coal.|
34554|Sue Group|69081|5|Briefly described|p737 Fig.1|Lopingian||Geol. Prov: Perth Basin.|||Willespie Formation, Redgate Coal Measures, Ashbrook Sandstone, Rosabrook Coal Measures, Woodynook Sandstone.|||23-JUL-15
34554|Sue Group|69182|5|Briefly described|Ch2 p9, Ch2 p11, Ch2 p34-p41|Late Permian|Early Permian|Southern Perth Basin. Fair to good porosity that is generally greater than 10 percent, however permeability is often poor due to cementation. See also Ch2 p44-p46, Ch2 p48, Ch2 p54, Ch2 p57, Ch2 p60, Ch2 p64-p66,Ch2 p80, Ch2 p83-p84, Ch2 p88-p91, Ch2 p92, Ch2 p94-p96, Ch2 p98, Ch2 p100, Ch2 p102, Ch2 p104, Ch2 p106, Ch2 p108-p110.|||Includes the Rosabrook Coal Measures, Ashbrook Sandstone, Redgate Coal Measures and the Willespie Formation.|Overlies the Stockton Group. Unconformably overlain by the Sabina Sandstone. Grades laterally into the Irwin River Coal Measures, High Cliff Sandstone and the Carynginia Formation.|Sandstone and siltstone interbedded with minor thin coals.|
34554|Sue Group|69297|6|Mentioned|p175,  p189, p190|Changhsingian|Sakmarian|Vlaming Sub-basin, South Perth Basin. |||Includes the Woodynook Sandstone, Rosabrook Coal Measures, Ashbrook Sandstone, Redgate Coal Measures and the Willespie Formation.|||
34554|Sue Group|70097|5|Briefly described|p6, p19 Fig.3|Wuchiapingian|Sakmarian|Southern Perth Basin. Mandurah Terrace and Bunbury Trough.|||Woodynook Sandstone, Rosabrook Coal Measures, Ashbrook Sandstone, Redgate Coal Measures, Willespie Formation|Overlies Stockton Group. Is overlain by Sabina Sandstone.||12-SEP-17
34554|Sue Group|70099|5|Briefly described|Fig.4|Wuchiapingian|Sakmarian|Mentelle 1A and 1B Supersequences.|||Woodynook and Ashbrook Sandstones; Rosabrook and Redgate Coal Measures; Willespie Formation.|Overlies Stockton Group.||
34554|Sue Group|70128|5|Briefly described|p449, p451|Permian|Permian|Perth Basin. Formerly the Sue Coal Measures.|||Woodynook, Ashbrook Sandstones; Rosabrook, Redgate, Coal Measures; Willespie Formation.|Is overlain conformably by Sabina Sandstone.||
34554|Sue Group|71377|5|Briefly described|p7, p77|||Mandurah Terrace, Perth Basin.|||Includes the Willespie Formation.|Conformably overlain by the Sabina Sandstone.||
34554|Sue Group|71958|5|Briefly described|p34|Changhsingian|Sakmarian|Vlaming Sub-basin.|||Includes the Woodynook Sandstone, Rosabrook Coal Measures, Ashbrook Coal Measures, Redgate Coal Measures and the Willespie Formation.|Overlies the Mosswood Formation. Overlain by the Sabina Sandstone.||
32237|Sulphur Springs Group|23206|6|Mentioned|Fig.1|||Age: 3.24 Ga.||||||
32237|Sulphur Springs Group|23416|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup, Pilbara Craton.||||||07-NOV-08
32237|Sulphur Springs Group|23484|5|Briefly described|p23|Archean|Archean|Age: c. 3260 -3235Ma.   Geological Province: Pilbara Craton.||||||07-NOV-08
32237|Sulphur Springs Group|23755|4|Described|p36|Archean|Archean|See also page 17 table 1.||||||07-NOV-08
32237|Sulphur Springs Group|23757|5|Briefly described|p10|Archean|Archean|Disconformably overlies Sulphur Springs Group. Age: c.3255-3235 Ma (SHRIMP U-Pb zircon).||||||07-NOV-08
32237|Sulphur Springs Group|23783|4|Described|p16|Archean|Archean|Of Pilbara Supergroup.||||||07-NOV-08
32237|Sulphur Springs Group|23784|5|Briefly described|p2|Archean|Archean|Age: 3240Ma.||||||07-NOV-08
32237|Sulphur Springs Group|23793|4|Described|p14|Archean|Archean|Age: 3260-3235Ma||||||07-NOV-08
32237|Sulphur Springs Group|23807|5|Briefly described|p110|Archean|Archean|Age: 3240Ma (Buick et al, 2001).  See also Sulphur Spring Group.||||||07-NOV-08
32237|Sulphur Springs Group|23813|5|Briefly described|p101|Archean|Archean|Age: c.3.24-3.25Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.  See also P91 Tb. 1.||||||07-NOV-08
32237|Sulphur Springs Group|23891|4|Described|p90|Archean|Archean|Ages: 3235+/-3Ma and 3238+/-3Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
32237|Sulphur Springs Group|23936|4|Described|p2, Tb.1|Archean|Archean|Age: ca. 3255-3235 Ma. Geological Province: Pilbara Craton. Underlying Unit: Warrawoona Group (unconformably). Overlying Unit: Gorge Creek Group (disconformably).||||||07-NOV-08
32237|Sulphur Springs Group|23956|4|Described|p1264|||Unconformably overlies the Warrawoona Group. Overlain by the Gorge Creek Group. Geological Province: Pilbara Craton.||||||
32237|Sulphur Springs Group|24025|4|Described|p8 Tb. 1|Archean|Archean|Includes the Kangaroo Caves, Kunagunarinna and Leilira Formations.  Age: c.3255-3235Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
32237|Sulphur Springs Group|24110|5|Briefly described|Plate 1|Archean|Archean|Parent: Pilbara Supergroup.  Geological Province: Pilbara Craton.||||||07-NOV-08
32237|Sulphur Springs Group|24166|5|Briefly described|p3|Archean|Archean|Age: 3280-3235Ma||||||07-NOV-08
32237|Sulphur Springs Group|24184|5|Briefly described|p702, p699 Fig.3|Archean|Archean|Parent: Pilbara Supergroup. Underlying Unit: Euro Basalt. Geological Province: Pilbara Craton. Age: ca. 3.26-3.24Ma. Lowermost Six Mile Creek Formation reassigned to underlying Euro Basalt (GSWA, unpub. data).||||||07-NOV-08
32237|Sulphur Springs Group|24185|5|Briefly described|p735 Fig.2, p739 Tb.3|Archean|Archean|Age: ~3240 Ma (Vearncombe et al, 1998); 3238 +/- 2 (SHRIMP zircon U-PB Buick et al, 2002). Geological Province: Pilbara Craton.||||||07-NOV-08
32237|Sulphur Springs Group|24186|5|Briefly described|p776, 777 Fig.2|Archean|Archean|Locally overlies Warrawoona Group unconformably. Geological Province: Pilbara Craton.||||||07-NOV-08
32237|Sulphur Springs Group|24187|5|Briefly described|p776, 777 Fig.2|Archean|Archean|Age: ca. 3235 Ma (U-Pb, Buick et al, 2002). Geological Province: Pilbara Craton||||||07-NOV-08
32237|Sulphur Springs Group|24531|4|Described|p18|Archean|Archean|Of the Pilbara Supergroup. Disconformably overlain by the Gorge Creek Group. Age: c.3255-3235 Ma. Geological Province: Pilbara Craton. See also p6.||||||07-NOV-08
32237|Sulphur Springs Group|24532|5|Briefly described|Map legend|Archean|Archean|Of the Pilbara Supergroup.  Age: c.3240Ma.||||||07-NOV-08
32237|Sulphur Springs Group|24541|6|Mentioned|p38|||Geological Province: East Pilbara Granite-Greenstone Terrane.||||||
32237|Sulphur Springs Group|24550|5|Briefly described|p30, p31 Tb. 3.1|Archean|Archean|Age: ca 3.23Ga. Geological Province: Pilbara Craton.||||||07-FEB-11
32237|Sulphur Springs Group|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Overlies Salgash Subgroup; underlies Gorge Creek Group. Ages: >3238-3235Ma and 3260-3240Ma. Geological Province: Pilbara Craton. See also p28 Fig. 1.2 .||||||07-FEB-11
32237|Sulphur Springs Group|24621|5|Briefly described|p81|Archean|Archean|Age: <3.24Ga.  Geological Province: Pilbara Craton.||||||07-NOV-08
32237|Sulphur Springs Group|50379|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
32237|Sulphur Springs Group|50423|4|Described|p216||Archean|3240 Ma. Volcanism followed hiatus after deposition of Wyman Formation. East Pilbara Granite-Greenstone Terrane.||||||03-DEC-14
32237|Sulphur Springs Group|50427|4|Described|p182 Fig.2|Archean|Archean|Age: 3250-3230 Ma. Overlies Golden Cockatoo Formation (generally conformable) and Budjan Creek Formation and Kelley Subgroup (unconformably). Overlain by Gorge Creek Group (conformably and unconformably). Of Pilbara Supergroup.||||||07-NOV-08
32237|Sulphur Springs Group|50430|4|Described|p158 Tb.1||Archean|Deposited 3235-3280 Ma. Volcanic. Unconformably overlies Euro Basalt. In East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
32237|Sulphur Springs Group|50544|5|Briefly described|p18, p40|Archean|Archean|Of the Pilbara Supergroup.  Age: c.3.26-3.24Ga.  Age given as c.3235Ma at centre of thre East Pilbara Granite-Greenstone Terrane (Van Kranendonk, 200;  Van Kranendonk et al, 2001).   Not on the YARRIE sheet.||||||07-NOV-08
32237|Sulphur Springs Group|60112|6|Mentioned|p107 Fig.1. |||||||||
32237|Sulphur Springs Group|61111|5|Briefly described|p96 Fig.2||Paleoarchean||c.3240 Ma.|||||
32237|Sulphur Springs Group|61205|4|Described|p548 Fig. 1|||Geological Province: Pilbara Craton. Overlain disconformably by Gorge Creek Group. Includes Strelley Granite and Kangaroo Caves Formation. Hosts a massive sulfide deposit. Interbedded volcanic and sedimentary rocks.||||||31-MAY-07
32237|Sulphur Springs Group|61253|5|Briefly described| p50, p52 Fig. 2, p58|Archean|Archean|Of Pilbara Supergp. Comprises Leilira (at base), Kunagunarinna and Kangaroo Caves Fms: previously incl.at its base, Six Mile Creek Fm (due to chem.similiarities now incl.with Euro Basalt. Unconform. on Kelly Gp. Age: c3.25-3.24Ma.Geol.Prov:Pilbara Craton.||||||07-NOV-08
32237|Sulphur Springs Group|61256|5|Briefly described|p339, p340 Fig. 5|Archean|Archean|Includes the Leilira, Kunagunarrina and Kangaroo Caves Fms.  A komatiite through rhyolite succession, and deep water hydrothermal system.  Unconformably overlies Euro Group rocks.  Age: ca. 3.24Ga.  Geological Province: Pilbara Craton.  See also p348.||||||07-NOV-08
32237|Sulphur Springs Group|61266|4|Described|p55, p59|Archean|Archean|Age: c. 3240 Ma. Unconformably to paraconformably overlies Warrawoona Group. Conformably to disconformably underlies Gorge Creek Group. Geological Province: Pilbara Craton. See also p58 Tb.1e||||||07-NOV-08
32237|Sulphur Springs Group|61579|5|Briefly described|p58 Fig. 2|Archean|Archean|Unconformably overlies the Warrawoona Group; unconformably overlain by Gorge Creek Group. ||||||07-NOV-08
32237|Sulphur Springs Group|63245|5|Briefly described|p4 Fig. 1|Archean|Archean|Age: c.3240Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
32237|Sulphur Springs Group|63417|5|Briefly described|Map legend|Archean|Archean|Of the Pilbara Supergroup. Includes Budjan Creek Formation. Age: <3228Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
32237|Sulphur Springs Group|63420|5|Briefly described|Map legend|Archean|Archean|Of the Pilbara Supergroup. Includes Leilira, Kunagunarrina and Kangaroo Caves Formations, and Farrel Quartzite. Ages: c3255Ma and c.3240-3235Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
32237|Sulphur Springs Group|63441|3|Fully described|p4 Tb. 1, p21|Archean|Archean|Of Pilbara Supergp. Incl: Leilira, Kunagunarinna + Kangaroo Caves Fms; + newly added Budjan Creek Fm. Formerly incl. Six Mile Creek Fm, now assigned to Euro Basalt.Overlies Kelly Gp; unconformable below Soanesville Gp. Age:3250Ma. Max.thick: 3000m.||||||07-FEB-11
32237|Sulphur Springs Group|63538|4|Described|p2 Fig. 1, p3 Fig. 2, p5, p10, p15|Archean|Archean|Of Pilbara Supergroup. Includes Kunagunarrina Formation. Disconformably underlain by Kelly Group. Overlain by Soanesville Group. Age: 3270-3230Ma. Thick: 4000m. Geological Province: Pilbara Craton. Komatiitic through rhyolitic volcanic succession.||||||19-APR-13
32237|Sulphur Springs Group|63649|5|Briefly described|p201 Fig. 2|Archean|Archean|Of Pilbara Supergroup. Contains Kangaroo Caves Formation. Geological Province: Pilbara Craton.||||||07-FEB-11
32237|Sulphur Springs Group|64328|5|Briefly described|p56 Tb. 1|||Includes Leilira, Kunagunarrina and Kangaroo Caves Formations.||||||07-FEB-11
32237|Sulphur Springs Group|64405|5|Briefly described|p2 Fig. 1|Archean|Archean|Of the Pilbara Supergroup. Geological province: East Pilbara Terrane.||||||07-FEB-11
32237|Sulphur Springs Group|64580|4|Described|map legend||Paleoarchean|Of Pilbara Supergroup. Mafic and felsic volcanic rocks; minor sedimentary rock; metamorphosed.||||||22-OCT-08
32237|Sulphur Springs Group|64632|6|Mentioned|p201 Fig.1, p202|Paleoarchean|Paleoarchean|East Pilbara terrane. Up to 4km thick.|3270-3235 Ma|Of the Pilbara Supergroup.||Overlies Kelly Group. Overlain by Soanesville Group.|Komatiitic to rhyolitic volcanic rocks.|
32237|Sulphur Springs Group|64747|6|Mentioned|p94 fig 1|Paleoarchean|Paleoarchean||c.3240 Ma.|||||
32237|Sulphur Springs Group|65008|6|Mentioned|p13|||||||Disconformably overlain by the Gorge Creek Group.||
32237|Sulphur Springs Group|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of Pilbara Supergroup.|Includes Budjan Creek Formation.|||
32237|Sulphur Springs Group|65757|5|Briefly described|p83 Fig.3, p84||Paleoarchaen|volcanics. Age: 3251-3235, unconformably overlain by the Soanesville Group.||||||
32237|Sulphur Springs Group|65825|6|Mentioned|p5. |Archean|Archean|||Unit in Pilbara Supergroup according to Van Kranendonk et al. (2001, 2002).||Intruded by Cleland Supersuite.||12-MAY-20
32237|Sulphur Springs Group|65827|5|Briefly described|p6 Tb.1, p28|Paleoarchean|Paleoarchean|Of Pilbara Supergroup; includes Budjan Creek Formation. 3250-3235 Ma (Buick et al. 2002).||||||21-JAN-22
32237|Sulphur Springs Group|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit of Pilbara Supergroup. Includes Leilera, Kunagunarrina, Kangaroo Caves (with its Pincunah Banded-iron Member), and Budjan Creek Formations, as well as an unnamed unit of metamorphosed mafic and felsic volcanic rocks with minor sedimentary rock.||||||
32237|Sulphur Springs Group|66118|4|Described|p146 Fig.1, p147-149|||Pilbara Craton. East Pilbara Terrane. Shown in Fig.1 as Sulphur Springs. Shown as Warrowoona, Kelly, and Sulphur Springs Group in Fig.2.|c. 3240 Ma; 3270-3240 Ma|Pilbara Supergroup||Is disconformably to unconformably overlain by Soanesville Group (onlapping lower disconformable contact). Unconformably overlies Kelly Group.|Plume-derived succession of ultramafic through rhyolitic volcanic rocks. Silicified epiclastic rocks at top of dominantly volcanic|
32237|Sulphur Springs Group|66122|6|Mentioned|p74|Archean|Archean||3.27 - 3.23 Ga.|Pilbara Supergroup.||||
32237|Sulphur Springs Group|66217|4|Described|p8, p10, p12, p14, p36.|Paleoarchean|Paleoarchean|Eastern Pilbara Craton. Hosts volcanigenic massive sulfide deposits. Interpreted as either back-arc sequence, or an upward-fractionating, plume-derived volcanic sequence affected by increasing degrees of crustal contamination. Eruption was contemporaneous with intrusion of Cleland Supersuite.|3.27-3.24 Ga.|||Unconformably overlies Kelly Group.|Basal unit of clastic sedimentary rocks, overlain by a 4 km thick succession of komatiite, komatiitic basalt, basaltic andesite, dacite and rhyolite.|10-JUN-20
32237|Sulphur Springs Group|66664|6|Mentioned|p3.  |||East Pilbara Terrane||Part of Pilbara Supergroup.||||
32237|Sulphur Springs Group|66745|4|Described|pp50-59.|Paleoarchean|Paleoarchean|Volcanic formations overlying a basal sedimentary formation, the Leilira Formation. The Budjan Creek Formation has been removed from this Group and reassigned to the Soanesville Group on the basis of its sedimentology and interpreted tectonic setting.|3270-3235 Ma. |Unit in Pilbara Supergroup.|Includes Leilira, Kunagunarinna and Kangaroo Caves Formations.|Unconformably overlies Kelly Group. Is overlain by Soanesville Group.||
32237|Sulphur Springs Group|66887|5|Briefly described|p21 Fig.11|||Pilbara Craton.|~3257-~3240 Ma estimated from Fig.11.|||||
32237|Sulphur Springs Group|67130|5|Briefly described|p16, p17|Paleoarchean|Paleoarchean|Deposited unconformably on older greenstones. Up to 4km thick in the type area.|3270 Ma - 3230 Ma|Pilbara Supergroup|Includes Leilira Formation,  Kunagunarrina Formation, Kangaroo Caves Formation|Intruded by Strelley Monzogranite, disconformably overlain by Soanesville Group, overlies Kelly Group||
32237|Sulphur Springs Group|67197|5|Briefly described|p2-5|Paleoarchean|Paleoarchean|Pilbara Craton.|3270-3235 Ma.|Pilbara Supergroup.|Leilira, Kunagunarrina, Kangaroo Caves Formations.|Unconformably overlies Kelly Group.||
32237|Sulphur Springs Group|67201|4|Described|p7 Fig.4, p10-12, p26|||In northern Pilbara Craton, East Pilbara Terrane.|3270-3235 Ma|Uppermost group in Pilbara Supergroup|Kangaroo Caves Formation, Kunagunarrina Formation, Leilira Formation|Erosionally overlies Kelly Group. Tectonic contact above.|Conglomerate, sandstone, and volcaniclastic rocks at base; upper part composed of komatiite and komatiitic basalt, overlain by basalt, andesite, dacite, rhyolite, and chert.|25-NOV-16
32237|Sulphur Springs Group|67269|5|Briefly described|p6 Fig.3|Paleoarchean|Paleoarchean||||Leilira, Kunagunarinna, Kangaroo Caves Formations.|Overlies Kelly Group.||
32237|Sulphur Springs Group|67270|5|Briefly described|p2-4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Pilbara Supergroup.|Leilira, Kunagunarinna, Kangaroo Caves Formations.|Unconformably overlies Kelly Group.||
32237|Sulphur Springs Group|67668|5|Briefly described|Fig. 2; p. 154, 157; Tb.1. ||Paleoarchean|East Pilbara Terrane, Pilbara Craton. Contains one of Earth's oldest massive sulfide deposits (Vearnacombe et al. 1995).|3270 - 3240 Ma.|Pilbara Supergroup|Leilira Formation, Kunagunarrina Formation, Kangaroo Caves Formation|Underlies the Soanesville Group, overlies the Kelly Group unconformably.|A mixture of sedimentary and volcanic rocks.|
32237|Sulphur Springs Group|68035|5|Briefly described|p287,  p286 Fig 3, p288 Fig 4|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|max age 3255 Ma, min age < 3235 Ma|Of Pilbara Supergroup.|Includes Kunagunarinna  Formation, Kangaroo Caves Formation.|Unconformably overlies Kelly Group. Associated with Cleland Supersuite.||
32237|Sulphur Springs Group|68280|6|Mentioned|p3, p4||||||Includes Leilira Formation, Kunagunarinna Formation, Kangaroo Caves Formation|||
32237|Sulphur Springs Group|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c.3255-3235 Ma.|Of the Pilbara Supergroup.|Includes Kangaroo Caves Formation, Kunagunarrina Formation, Leilira Formation.|||02-DEC-14
32237|Sulphur Springs Group|68282|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|3290-3220 Ma|Of the Pilbara Supergroup|Includes Kangaroo Caves Formation, Kunagunarrina Formation, Leilira Formation.|||
32237|Sulphur Springs Group|68283|5|Briefly described|Map Legend|Archean|Archean|East Pilbara Terrane, Pilbara Craton.||Of the Pilbara Supergroup.|Includes Kangaroo Caves Formation, Kunagunarrina Formation, Leilira Formation.|||23-SEP-13
32237|Sulphur Springs Group|68284|5|Briefly described|p7|Paleoarchean|Paleoarchean|Pilbara Craton.|3255-3235 Ma.|Pilbara Supergroup.|Leilira, Kunagunarinna, Kangaroo Caves, Formations.|Locally, unconformably overlies Kelly Group.||
32237|Sulphur Springs Group|69013|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Of the Pilbara Supergroup.|Includes Kangaroo Caves, Kunagunarrina and Leira Formations.|||30-APR-14
32237|Sulphur Springs Group|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Pilbara Supergroup.|Includes the Kangaroo Caves Formation, Kunagunarrina Formation, and Leilira Formation.|||
32237|Sulphur Springs Group|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Age derived from sample of metamorphosed felsic volcanic rock (160258.1.pdf) and constrains age of protolith crystallisation.|3253 Ma +/- 4 Ma (SHRIMP)|Pilbara Supergroup|Includes Kangaroo Caves Formation, Kunagunarrina Formation, Leilira Formation||Interlayered units of mafic and felsic schist.|
32237|Sulphur Springs Group|69185|4|Described|GEOL_LUT_CSV files||Paleoarchean|Geological province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 3255-3235 Ma|Unit of Pilbara Supergroup.|||Mafic and felsic volcanic rocks; minor sedimentary rock; metamorphosed|
32237|Sulphur Springs Group|69301|4|Described|p5 Fig.3, p9 Tb.1, p13, p20-21|||Pilbara Craton. East Pilbara Terrane.|3270-3235 Ma from unit ages|Pilbara Supergroup|Kangaroo Caves Formation, Kunagunarinna Formation, Leilira Formation|Is unconformably overlain by Soanesville Group. Unconformably overlies Kelly Group.||
32237|Sulphur Springs Group|69548|5|Briefly described|p1-4, 7-11|||Soanesville greenstone belt, East Pilbara terrane. Contains filaments of pyrite previously interpreted as thermophilic microbial communities. The authors regard the evidence as not compelling. Photomicrographs.|~3270-3230 Ma.||Kangaroo Caves Formation.|Overlies Warrawoona Group. Is overlain by Gorge Creek Group. Is intruded by Strelley Granite.|Wacke, mudrock, mafic volcanic rocks, intermediate volcanic rocks, felsic volcanic rocks, chert. Includes a VHMS deposit.|
32237|Sulphur Springs Group|69569|6|Mentioned|p285 Fig.1|||East Pilbara Terrane.||||||
32237|Sulphur Springs Group|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Occurs adjacent to, and is sheared by the Tabba Tabba Shear Zone. Sample GSWA 160258 (felsic metavolcanic rock) yielded an interpreted magmatic crystallisation age of 3253+\4 Ma for the volcanic rock (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|3255-3235 Ma (inferred)|Unit of Pilbara Supergroup.|Includes Kangaroo Caves Formation, Kunagunarrina Formation, Leilira Formation.|Intruded by c. 2590 Ma granites of the Sisters Supersuite.|Interlayered mafic and felsic schists|
32237|Sulphur Springs Group|69616|5|Briefly described|p160-165, p180|Archean|Archean|Thickness to 2500-3000m. Bulk of magmatism c.3240 Ma. Widespread alteration.|c.3255-3235 Ma (SHRIMP U-Pb zircon).||Includes Leilira, Kunagunarrina and Kangaroo Caves Formations.|Unconformably overlies Kelly Group.||
32237|Sulphur Springs Group|70022|5|Briefly described|p114-115|||East Pilbara Terrane.|3250 Ma.|Pilbara Supergroup.|Leilira, Kunagunarinna, Kangaroo Caves Formations.|Unconformably overlies Kelly Group. Is overlain unconformably by Soanesville Group.||
32237|Sulphur Springs Group|70729|6|Mentioned|p163-164|||Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Pilbara Supergroup.||||
32237|Sulphur Springs Group|70733|6|Mentioned|p105|||Eastern Pilbara Craton.||Pilbara Supergroup.||||
32237|Sulphur Springs Group|70775|6|Mentioned|iv, p12, p24-p25, p68, p78, p80, p100|||In the type area hosts VHMS mineralization.|3275-3235 Ma|Pilbara Supergroup|Includes the Kangaroo Caves Formation, Kunagunarinna Formation and the Leilira Formation.|Unconformably overlies the Kelly Group. Unconformably overlain by the Soanesville Group.||
32237|Sulphur Springs Group|70826|6|Mentioned|p8|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Time equivalent of the Roebourne Group.||Pilbara Supergroup||||12-MAY-20
32237|Sulphur Springs Group|70884|5|Briefly described|p123|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Pilbara Supergroup.|Includes Kangaroo Caves, Kunagunarinna and Leilira formations.|Underlain by Kelly Group.||
32237|Sulphur Springs Group|71041|6|Mentioned|p45 fig 2|Paleoarchean|Paleoarchean||3240 Ma|Of Pilbara Supergroup.|Includes the Kangaroo Caves Formation.|Overlain by the Soanesville Group.||10-NOV-17
32237|Sulphur Springs Group|71137|6|Mentioned|p4|Archean|Archean|Pilbara. Appears mis-spelt as Sulfur Springs Group.|||Kangaroo Caves Formation.|||
32237|Sulphur Springs Group|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||acid and basic volcanic rock, greywacke, sandstone, diorite sills, metadiorite|
32237|Sulphur Springs Group|71487|5|Briefly described|p128|Archean|Archean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Pilbara Supergroup.||Uppermost unit of Pilbara Supergroup. Overlain by Soanesville Goup. Underlain by Kelly Group.||
32237|Sulphur Springs Group|72034|6|Mentioned|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Kangaroo Caves Formation, Kunagunarrina Formation, Leilira Formation.|||
32237|Sulphur Springs Group|72064|5|Briefly described|p66|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Pilbara Supergroup.|Incldues Kangaroo Caves, Kunagunarinna and Leilira formations.|Underlain by Kelly Group.||
32237|Sulphur Springs Group|72251|5|Briefly described|p52-54|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|3250 Ma|Unit of Pilbara Supergroup.|Includes Cangaroo Caves, Kunagunarinna and Leilira formations.|Uppermost unit of Pilbara Supergroup. Overlain unconformably by Soanesville group. Underlain unconformably by Kelly Group.||
32237|Sulphur Springs Group|72668|4|Described|p3-9, p14, p24, p27-28|||Deposited unconformably on the older greenstones in the western part of the East Pilbara Terrane where it is up to 4000m thick. Type area occurs in the Soanesville greenstone belt. Geochemistry is discussed.|<3270-3230 Ma|Pilbara Supergroup|Includes the Kangaroo Caves Formation, Kunagunarrina Formation and the Leilira Formation.|Disconformably overlain by the Soanesville Group.||14-JAN-22
32237|Sulphur Springs Group|73598|5|Briefly described|p1207, 1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.|3230 Ma.|Pilbara Supergroup.|Leilira, Kunagunarinna, Kangaroo Caves Formations.|Unconformably overlies Kelly Group. Is overlain unconformably by Soanesville Group.||
33753|Sunbeam Group|22896|6|Mentioned|103|||Geol province Officer Basin||||||
33753|Sunbeam Group|22907|3|Fully described|40|||Geol province Officer Basin. Age ~800 Ma. Overlying units Disappointment Group & Boondawari Formation, Underlying unit Manganese Group||||||
33753|Sunbeam Group|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Officer Basin.||||||
33753|Sunbeam Group|23529|5|Briefly described|p7|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin||||||
33753|Sunbeam Group|23590|5|Briefly described|p16|Neoproterozoic|Neoproterozoic|Previously Savory Group.  Geological Province: Officer Basin.||||||
33753|Sunbeam Group|23730|4|Described|p12|Neoproterozoic|Neoproterozoic|Age: c.830-700 Ma. Geological Province: Officer Basin.||||||
33753|Sunbeam Group|23758|5|Briefly described|p2 Fig 1|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
33753|Sunbeam Group|23760|4|Described|p30|Neoproterozoic|Neoproterozoic|Incorporates the superseded Savory Group. Age: c.800 Ma. Geological Province: Officer Basin.||||||
33753|Sunbeam Group|24017|6|Mentioned|p5 Tb. 1|||Superseded by Salvation Group.||||||
33753|Sunbeam Group|24018|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
33753|Sunbeam Group|24115|5|Briefly described|p2|Neoproterozoic|Neoproterozoic|Overlies the rocks of the Bangemall Supergroup succession. Geological Province: Officer Basin.||||||
33753|Sunbeam Group|24161|5|Briefly described|p7|Neoproterozoic|Neoproterozoic|Unconformably overlies the Collier Group. Geological Province: Officer Basin.||||||
33753|Sunbeam Group|24183|5|Briefly described|p6|Neoproterozoic|Neoproterozoic|||||||
33753|Sunbeam Group|24535|5|Briefly described|p1, 2, p4 Fig. 2, p5|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin. Unconformably overlies Bangemall Supergroup. Previously included Coonabildie, Brassey Range and Jilyili Formations||||||26-NOV-13
33753|Sunbeam Group|24578|5|Briefly described|p776 Fig.1|Neoproterozoic|Neoproterozoic|Age: 820 Ma. Geological Province: Officer Basin.||||||
33753|Sunbeam Group|24594|5|Briefly described|p602|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin (Paterson Orogen).||||||
33753|Sunbeam Group|49895|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Geological Province: Savory Basin/Officer Basin. Part of this unit was formerly the "lower Savory Group". See also p12 Tb. 1.||||||
33753|Sunbeam Group|50008|5|Briefly described|p44|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
33753|Sunbeam Group|50188|5|Briefly described|p2 Fig. 1, p15, p17|Neoproterozoic|Neoproterozoic|Together with Disappointment Group replaced some of the rocks of the former 'Savory Group'. Geological Province: Officer Basin. Age: 825Ma (Bagas et al, 1999)||||||16-JUL-08
33753|Sunbeam Group|50226|6|Mentioned|p424 Fig. 5|||Geological Province: Officer Basin.||||||
33753|Sunbeam Group|50228|5|Briefly described|p480 Fig.3|||Part of Supersequence 1.||||||24-JAN-06
33753|Sunbeam Group|50334|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin, Centralian Superbasin.||||||
33753|Sunbeam Group|60470|6|Mentioned|p3, Fig. 1|Neoproterozoic|Neoproterozoic|in Officer Basin||||||
33753|Sunbeam Group|61564|5|Briefly described|p590 Fig. 2|Neoproterozoic|neoproterozoic|Age: 820Ma.  Geological Province: Officer Basin.||||||
33753|Sunbeam Group|61732|5|Briefly described|p58 Fig. 22, p85|Cryogenian|Cryogenian|Includes Coondra, Spearhole and Watch Point Formations, and the Mundadjini and Skates Hills Formations. Geological Province: western Officer Basin.||||||07-FEB-11
33753|Sunbeam Group|62453|4|Described|p5 Fig. 3, 22, 52|Cryogenian|Tonian|Geological Province: Officer Basin. Underlies Boondawarri Formation. Incorporates most older parts of the 'Savory Group'. Thickness = 4000-5000m. Correlates with Buldya Group. Superseded lower Savory Group. Includes Coonabildie Formation.||||||17-JUL-08
33753|Sunbeam Group|62987|5|Briefly described|p30|Neoproterozoic|Neoproterozoic|Includes Watch Point, Coondra, Spearhole, Mundadjini and Skates Hills Formations. Geological Province: Officer Basin.||||||
33753|Sunbeam Group|63022|5|Briefly described|p1014|||Age: ca830 to ca700Ma. Geological Province: Officer Basin.||||||10-AUG-07
33753|Sunbeam Group|64103|5|Briefly described|p400, p400 Fig. 3|Cryogenian|Tonian|Geological Province: Officer Basin. A sandier equivalent of the Buldya Group.||||||07-FEB-11
33753|Sunbeam Group|64283|5|Briefly described|p49, p51 Fig. 2|Neoproterozoic|Neoproterozoic|Overlain by Boondawarri Fm.Age:<830Ma.Geol. Province: Officer Basin. Dominated by shallowly dipping, moderately indurated quartz sandstone, with a basal cobble conglomerate, and a higher interval of stromatolitic carbonate forming Skates Hills Formation.||||||07-FEB-11
33753|Sunbeam Group|64284|5|Briefly described|p58 Fig. 1, p62 Fig. 3|||Geological Province: Officer Basin.||||||07-FEB-11
33753|Sunbeam Group|64285|5|Briefly described|p67 Fig. 2|||Geological Province: Officer Basin.||||||07-FEB-11
33753|Sunbeam Group|64286|5|Briefly described|p72, p73 Fig. 1|Neoproterozoic|Neoproterozoic|Comprises Brassey Range, Skates Hills and Boondawarri Formations. Geological province: Officer Basin. Contains evaporites at top. See also p75 Fig. 3, p76 Fig. 4.||||||07-FEB-11
33753|Sunbeam Group|64580|6|Mentioned|map legend||Neoproterozoic|||||||
33753|Sunbeam Group|64722|6|Mentioned|Fig. 6 p15|Neoproterozoic|Neoproterozoic|Of Yeneena Basin? Centralian Superbasin.||||||
33753|Sunbeam Group|64725|6|Mentioned|p67.|Neoproterozoic|Neoproterozoic|||||||
33753|Sunbeam Group|64772|5|Briefly described|p13, p15, Plate 1, p20-21, p33, p45|Neoproterozoic|Neoproterozoic|Includes Watch Point, Coondra, Spearhole, Mundadjini + Skates Hills Fms. Overlain by Boondawari Fm. Age: c.820Ma. Geol.prov: Officer Basin. Equivalent to Depositional Sequence B of Williams (1992). Presented as Upper+ Lower Sunbeam Groups in Fig. 7, p14.||||A lateral equivalent of  Buldya Group.|Sandstone, siltstone, conglomerate, shale, mudstone, dolomite, stromatolitic dolomite, and evaporitic rocks|25-NOV-13
33753|Sunbeam Group|64777|5|Briefly described|p2 Fig.3, p4 |Neoproterozoic|Neoproterozoic|Includes 800 Ma stromatolitic assemblages (Grey and Stevens 1997, Stevens and Grey 1997).|ca. 800 Ma|||||
33753|Sunbeam Group|65363|6|Mentioned|pp18-19.|||Appears to be stratigraphically lower than Kanpa Formation.||||||
33753|Sunbeam Group|65454|5|Briefly described|p6, p7 Fig.3, p11, p30 Fig.A1b|Cryogenian|Cryogenian|Of Officer Basin. Consists of Mundadjini Formation in the study area; includes Skates Hill Formation in NW Officer Basin. Interpreted correlative of Supersequence 1 of Centralian Superbasin and Yeneena Basin sediments. Disconformably overlain by Disappointment Group. Age between 830 Ma and c.800 Ma.||||||
33753|Sunbeam Group|65472|6|Mentioned|p5 Fig. 4|||Officer Basin.||||||
33753|Sunbeam Group|65826|5|Briefly described|p3 Fig.1, p10. |Neoproterozoic|Neoproterozoic|Officer Basin.|c.820 - 654 Ma.|||||
33753|Sunbeam Group|67202|5|Briefly described|p64|||NW Officer Basin.|||Mundadjini Formation.|||
33753|Sunbeam Group|68270|5|Briefly described|p683|Tonian|Tonian|Western Officer Basin. ||||Overlain disconformably/unconformably by Sunbeam Group.||
33753|Sunbeam Group|69003|6|Mentioned|p4, p23, p60-61, p64|||Officer Basin, Paterson Orogen. Deformed by the c.650 Ma Miles Orogeny.||||||
33753|Sunbeam Group|69185|5|Briefly described|GEOL_LUT_CSV files|Neoproterozoic|Proterozoic|Of Officer Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|||Includes Coondra Formation, Mundadjini Formation, Spearhole Formation, Watch Point Formation.|||
33753|Sunbeam Group|69596|6|Mentioned|p4|Neoproterozoic|Neoproterozoic|Capricorn Orogen.||||||
33753|Sunbeam Group|70826|6|Mentioned|p5 tbl 2|||Supersequence 1, Centralian Superbasin.||||||20-APR-20
33753|Sunbeam Group|72034|6|Mentioned|500k_interpgeop16_lut|Tonian|Tonian|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Coondra Formation, Watch Point Formation, Skates Hills Formation, Mundadjini Formation.|||
74207|Sunbird Formation|61542|4|Described|p276, p277 Fig. 2, p285-6||Visean|Top unit of Weaber Group - forms part of revision by authors.Unconformably overlies Sandbar Sandstone and Tanmurra Fm. Geol. Province: Bonapart Basin/Petrel-Sub-basin. Detailed lithology included. type section described. 638-725 m in Bonaparte-1, onshore WA. Reference section in Sunbird-1, offshore NT.||||Unconformable on Tanmurra Fm. Nature of contact with underlying Sandbar Sst unknown.||26-NOV-18
74207|Sunbird Formation|67354|5|Briefly described|p73. |||||Unit in Weaber Group.||Is overlain by Wadeye Sub-Group.||
74207|Sunbird Formation|69452|5|Briefly described|p36:12, 14-15, 17|Carboniferous|Carboniferous|||Weaber Group.||Unconformably overlies Sandbar Sandstone and Tanmurra Formation.||12-JUL-16
74207|Sunbird Formation|69653|6|Mentioned|p10|Carboniferous|Carboniferous|Petrel Sub-basin.||Weaber Group.||Overlies Sandbar Sandstone. Is overlain by Arco Formation (Wadeye Group).||
74207|Sunbird Formation|69673|6|Mentioned|p168 fig 138, p171|Carboniferous|Carboniferous|||Weaber Group||||
74207|Sunbird Formation|70061|5|Briefly described|Petrel Sub-basin Fig.3|Serpukhovian|Visean|See also Regional geology: Fig.8.||Weaber Group.||Overlies Sandbar Sandstone. Is overlain by Arco Formation (Wadeye Group).||12-JUL-16
74207|Sunbird Formation|73117|6|Mentioned|p15|Visean|Visean|Bonaparte Basin, southern.||Weaber Group||Underlain by Tanmurra Formation. Equivalent to Sandbar Sandstone.||
75922|Surprise Orthogneiss|66113|5|Briefly described|Map legend|Archean|Archean|Burtville Terrane, Yilgarn Craton. Unit in Minigwal Suite. Age c.2765 Ma. Migmatitic quartz-biotite orthogneiss.||||||
75922|Surprise Orthogneiss|68107|5|Briefly described|p611, p616.|Neoarchean|Neoarchean|Cross-cut by c. 2645 Ma dykes.|ca. 2765 Ma (Fletcher et al. 2001).|Of the Minigwal Suite.||||
75922|Surprise Orthogneiss|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Burtville Terrane, Eastern Goldfields Superterrane, Yilgarn Craton||Minigwal Suite|||Migmatitic quartz-biotite orthogneiss.|07-AUG-15
75922|Surprise Orthogneiss|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|See also 100k_geologyp14_lut.csv and 500k_interpgeop14_lut.csv.|2769 - 2765 Ma (inferred).|Minigwal Suite|||Migmatitic quartz-biotite orthogneiss.|
75922|Surprise Orthogneiss|70802|4|Described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Burtville Terrane, Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events.|2769-2765 Ma (inferred)|Unit of Minigwal Suite.|||Migmatitic quartz-biotite orthogneiss|
75922|Surprise Orthogneiss|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Burtville Terrane, Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 100k_geologyp14_lut.csv, 500k_interpgeop_lut.csv.|2769-2765 Ma (inferred)|Unit of Minigwal Suite.|||Migmatitic quartz-biotite orthogneiss|
75922|Surprise Orthogneiss|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|||Minigwal Suite|||Migmatitic quartz--biotite orthogneiss.|
22925|Survey Creek Monzogranite|23751|4|Described|p11|||Composed of weakly foliated, medium to coarse grained, porphyritic biotite-hornblende monzogranite and minor, even-textured monzogranite.||||||
22925|Survey Creek Monzogranite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
22925|Survey Creek Monzogranite|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
22925|Survey Creek Monzogranite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
22925|Survey Creek Monzogranite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Paperbark Supersuite|||Medium- to coarse-grained, porphyritic biotite-hornblende monzogranite.|04-AUG-15
22925|Survey Creek Monzogranite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Paperbark Supersuite|||Medium to coarse grained, porphyritic biotite-hornblende monzogranite.|
22925|Survey Creek Monzogranite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone.|1864-1852 Ma (Inferred)|Unit of Paperbark Supersuite.|||Medium- to coarse-grained, porphyritic biotite-hornblende monzogranite|
22925|Survey Creek Monzogranite|70154|6|Mentioned|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1852-1864 Ma|Paperbark Supersuite||||
22925|Survey Creek Monzogranite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (183 -1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1864-1852 Ma (inferred)|Unit of Paperbark Supersuite.|||Medium- to coarse-grained, porphyritic biotite-hornblende monzogranite|
22925|Survey Creek Monzogranite|72437|5|Briefly described|p86-87|||Lamboo Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Biotite monzogranite.|
69788|Swan River Formation|63745|2|Defined|p67-69, p74, p79 Appdx.|Late Pleistocene|Late Pleistocene|Unconformably overlies Kings Park Fm., Perth Fm. and Osborne Fm. Series of beds and lenses of estuarine and alluvial clean, coarse grey sands and gravels, and red, brown, yellow and black clays. Max. thickness: 26m. See also p59.||||||07-FEB-11
24004|Sweeney Mia Formation|1943|2|Defined|p388-389, p373, p375 Fig.3, p376 Fig 4|Devonian|Devonian|Type section in Yaringa-1 at 146-326m (Hocking, 1985). Max. thickness: 180m in Yaringa-1. Age: undated.||||Conformably overlies Kopke Sandstone. Correlation with Gneudna Formation preferred.|Sandstones.|20-JUN-13
24004|Sweeney Mia Formation|6943|5|Briefly described|p599, p601, pp604-606.|Devonian||Siltstone overlying breccia contains Frasnian fish scales.||||Overlies Kopke Sandstone. Is unconformably overlain by Winning Group.|Oxidised mixed carbonate and siliciclastics with minor evaporitic beds. Local intraformational dolomite clasts overlain by siltstone.|
24004|Sweeney Mia Formation|12729|4|Described|p. 11, 26, 28; Figs. 3-4, 6-8, 10, 22-4|Frasnian|Early Devonian|Central Gascoyne Platform. 192 m thick (max). Deposition: reducing, shallow lagoonal to supratidal. Stratigraphic position implies Early Devonian age, inferred correlation with upper Pragian regression. Worn Frasnian fish scales near formation top interpreted as a break in sedimentation.||||Conformably overlies the Kopke Sandstone.|Oxidized, mixed carbonate and siliciclastic rocks with minor evaporitic beds. Intraformational dolomite clasts.|
24004|Sweeney Mia Formation|12731|5|Briefly described|p590 Fig.2.|Early Devonian|Early Devonian|Dolomite might be a potential hydrocarbon reservoir.||||Overlies Kopke Sandstone.|Mixed siliciclastics and carbonates.|
24004|Sweeney Mia Formation|12733|5|Briefly described|p554 Fig.2.|Early Devonian|Early Devonian|Pragian-Emsian.||||Overlies Kopke Sandstone.|Mixed carbonate, clastic and evaporite sequence.|
24004|Sweeney Mia Formation|13615|6|Mentioned|p16|Devonian|Devonian|Of Iasky and Mory, 1999. Gascoyne Platform.||||||
24004|Sweeney Mia Formation|14228|5|Briefly described|p5 fig2, p6 fig3, p7, p18, p26|Emsian|Pragian|Gascoyne Platform. Up to 192 m thick. Dolomite and shale beds are a local aquiclude to Kopke Sandstone and a potential seal.||||Overlies Kopke Sandstone conformably.|Brown mudstone; light-grey to white, gypsiferous limestone; breccia; gypsum veins; thinly bedded sandstone.|
24004|Sweeney Mia Formation|22814|5|Briefly described|p256, fig2|Early Devonian|Early Devonian|Of Kalbarri Group?||||||
24004|Sweeney Mia Formation|23572|4|Described|p8 Fig. 6, p10|Emsian|Emsian|Geological Province: Carnarvon Basin. Underlying Unit: Kopke Sandstone (conformable). Max. thickness: 192m.||||||
24004|Sweeney Mia Formation|23935|5|Briefly described|p11 Fig.7|Emsian|Emsian|Conformably overlies Kopke Sandstone. Geological Province: Southern Carnarvon Basin.||||||
24004|Sweeney Mia Formation|24390|5|Briefly described|p19 Fig. 10||Devonian|Geological Province: Southern Carnarvon Basin.||||||
24004|Sweeney Mia Formation|40617|2|Defined|p3|Late Silurian|Late Silurian|||||||
24004|Sweeney Mia Formation|41271|3|Fully described|p41|||Formerly referred to as "Unknown formation, Unit A"||||||
24004|Sweeney Mia Formation|41438|6|Mentioned|p98|||See also Fig.5||||||
24004|Sweeney Mia Formation|42116|5|Briefly described|p9|||See also Fig.1||||||
24004|Sweeney Mia Formation|42441|4|Described|Fig.2 p3|||See also p87.||||||20-JUN-13
24004|Sweeney Mia Formation|49942|4|Described|p4 Fig.3, p9|Early Devonian|Early Devonian|Conformably overlies Kopke Formation. Max. thickness: 192 m. Oxidised carbonate and siliclastic rocks with minor evaporite beds, deposited in a reducing shallow-lagoonal to supratidal environment. Geological Province: Gascoyne Platform.||||||20-JUN-13
24004|Sweeney Mia Formation|50084|5|Briefly described|p77|Middle Devonian|Early Devonian|Geological Province: Southern Carnarvon Basin.||||||07-FEB-11
24004|Sweeney Mia Formation|50085|5|Briefly described|p19 Fig. 10|Devonian|Devonian|Geological Province: Southern Carnarvon Basin.||||||
24004|Sweeney Mia Formation|60384|5|Briefly described|p244, p243 Fig 2a|Early Devonian|Early Devonian|Southern Carnarvon Basin.||||Underlain by Kopke Sandstone|Oxidised carbonate and siliciclastic rocks with minor evaporite beds.|
24004|Sweeney Mia Formation|60725|5|Briefly described|p29, p33 Fig.4, p36 Fig.6. |Early Devonian|Early Devonian||||||Mixed carbonate, clastic, and evaporitic succession.|
24004|Sweeney Mia Formation|61023|5|Briefly described|p34 Fig. 14|Devonian|Devonian|Geological Province: Southern Carnarvon Basin.||||||11-APR-08
24004|Sweeney Mia Formation|61562|5|Briefly described|p547, p548|Middle Devonian|Middle Devonian|Age: ca. 380Ma.||||||
24004|Sweeney Mia Formation|61563|5|Briefly described|p583|Early Devonian|Early Devonian|Includes carbonates with a minor evaporite component.  See also p579 Fig. 3.||||||
24004|Sweeney Mia Formation|64635|6|Mentioned|p6 |||Has an erosion surface representing a substantial hiatus.|||||Marine, mixed siliciclastic-carbonate succession.|
24004|Sweeney Mia Formation|67200|5|Briefly described|p7 fig 5,p18 table 1, p55|Devonian|Devonian|Thermal conductivity of 2.78 W/mK||Kalbarri Group||Overlies Kopke Sandstone|Siltstone, dolomite and limestone with parallel cross bedding.|
24004|Sweeney Mia Formation|69029|6|Mentioned|p326|Emsian|Pragian|Of onshore Carnarvon Basin.||||Overlain by Nannyarra Sandstone. Underlain by Kopke Sandstone.||
24004|Sweeney Mia Formation|69182|5|Briefly described|Ch3 p8, Ch3 p10-p11|Middle Devonian|Early Devonian|Carnarvon Basin. Deposited in a reducing, shallow lagoonal or supra-tidal environment. Misspelt as the Sweeny Mia Formation in Ch3 p8. Unit relationship with the Kopke Sandstone is accidently given in reverse in Ch3 p10. See also Ch3 p23, Ch3 p35, Ch3 p37, Ch3 p67-p68, Ch3 p73.||||Conformably overlies the Kopke Sandstone.|Oxidized, mixed carbonate and siliciclastic rocks with minor evaporitic beds.|
24004|Sweeney Mia Formation|69297|6|Mentioned|p246, p249|Early Devonian|Early Devonian|Gascoyne Sub-basin of the Carnarvon Basin. Deposited in a shallow marine environment. ||||Overlies the Kopke Sandstone. Unconformably overlain by the Nannyarra Sandstone.|Mixed siliciclastics and dolomite.|
81551|Sweetwaters Well Dolomite|71270|4|Described|100k_geologyp14_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen. Of Earaheedy Basin. Events: Edmundian Orogeny (1026 - 954 Ma); Mangaroon Orogeny (1682 - 1619 Ma); Stanley Fold Belt deformation (2005 - 1620 Ma); Mangaroon Orogeny D2m/M2m (1677 - 1659 Ma); Mangaroon Orogeny D1m/M1m (1682 - 1677 Ma). |1990 Ma (inferred); 1949+\-10 Ma|Unit of Tooloo Subgroup.|||Stromatolitic dolomite and limestone; lesser siltstone and sandstone|
81551|Sweetwaters Well Dolomite|71484|4|Described|p122,124-125,130-131,137|Orosirian|Orosirian|Geological province: Of Earaheedy Basin. Contains stromatolitic carbonates at the top of the Yelma Formation dated at 2008+\-68 Ma and 1946+\-71 Ma (Pb-Pb model ages; Russell et al., 1994). Overlaps with recent U-Pb SHRIMP zircon ages of 1971+\-11 Ma, 1954+\-5 Ma and 1949+\-10 Ma from micro-tuff layers in the uppermost part of the unit (Sheppard et al., 2016).||Unit of Tooloo Group.||Overlain by Frere Formation. Underlain unconformably by Juderina Formation/Finlayson Member and Killara Formation.|Sandstone, dolomite (locally stromatolitic), siltstone, shale, minor conglomerate and limestone.|30-AUG-19
30666|Swift Monzogranite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1860Ma. Geological province: Kimberley Province (West).||||||07-FEB-11
30666|Swift Monzogranite|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|Approx 1865 - 1850 Ma.||||||
30666|Swift Monzogranite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite.||||||07-NOV-08
75246|Swincer Dolerite|66116|5|Briefly described|Map legend|Archean|Archean|Burtville Terrane, Yilgarn Craton. Comprises two units: metamorphosed dolerite, with minor basalt or gabbro components; and metamorphosed gabbro, with minor pyroxenite or quartz gabbro components. The latter has an age of 2812 +/- 5 Ma.||||||01-MAY-13
75246|Swincer Dolerite|66195|5|Briefly described|p610, p611 Fig.9|Mesoarchean|Mesoarchean|Burtville Terrane. 2812 +/- 5 Ma.||||||13-MAR-12
75246|Swincer Dolerite|67129|5|Briefly described|p55|Archean|Archean|Burtville Terrane, Eastern Goldfields Superterrane.|2812 +/- 5 Ma.|||||
75246|Swincer Dolerite|68107|4|Described|p607-608 Figs.3,4; p609 Table 1, p611.|Mesoarchean|Mesoarchean|Mount Sefton Greenstone Belt, Burtville Terrane. Laterally extensive mafic (?sub-volcanic) sills up to 250m thick. Fig.3 gives a much younger age of 2755 +/- 5 Ma .|2812 +/- 5 Ma (Wingate et al. 2011).||||Mafic rocks (undivided).|22-SEP-14
75246|Swincer Dolerite|68109|6|Mentioned|p665|Mesoarchean|Mesoarchean|Burtville Terrane. Contains zircons that show evidence of juvenile input.|ca. 2812 Ma|||||
75246|Swincer Dolerite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Merolia Domain, Burtville Terrane, Eastern Goldfields Superterrane, Yilgarn Craton|||||Dolerite; minor basalt or gabbro components; metamorphosed; gabbro; minor pyroxenite or quartz gabbro components; metamorphosed.|07-AUG-15
75246|Swincer Dolerite|69404|6|Mentioned|p4 Fig.4|Mesoarchean|Mesoarchean|Burtville Terrane.|c. 2800 Ma|||||
75246|Swincer Dolerite|69617|6|Mentioned|p154|||Burtville Terrane, Eastern Goldfields Superterrane.||||||
75246|Swincer Dolerite|70020|6|Mentioned|p132|||Geological province: Yilgarn Craton. Associated with c. 2.82 Ga plume magmatism in the Youanmi Terrane.||||||
75246|Swincer Dolerite|70153|5|Briefly described|100k_interpgeop_lut.csv|Mesoarchean|Mesoarchean|See also 100k_geologyp14_lut.csv and 500k_interpgeop14_lut.csv. Age derived from sample of pegmatitic metagabbro (185968.1.pdf)|2812 +/- 2 Ma (SHRIMP).||||Dolerite, gabbro; minor pyroxenite or quartz gabbro components; metamorphosed. Up to 250m thick.|
75246|Swincer Dolerite|70802|4|Described|500k_interpgeop14_lut.csv|Mesoarchean|Mesoarchean|Geological province: Burtville Terrane, Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events.|2812 Ma (inferred)||||Dolerite with minor gabbro; metamorphosed|
75246|Swincer Dolerite|70830|6|Mentioned|p28|Mesoarchean|Mesoarchean|Burtville Terrane.||||||
75246|Swincer Dolerite|71168|6|Mentioned|p10|Mesoarchean|Mesoarchean|Burtville Terrane, Yilgarn Craton.|2812 +/- 5 Ma|||||
75246|Swincer Dolerite|71270|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 100k_geologyp14_lut.csv, 500k_interpgeop_lut.csv.|2812+\-2 Ma||||Dolerite and gabbro; minor basalt, pyroxenite or quartz gabbro components; metamorphosed|
75246|Swincer Dolerite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Burtville Terrane.|||||Dolerite with minor gabbro; metamorphosed.|
75246|Swincer Dolerite|72491|6|Mentioned|p5 Fig.4|||Burtville Terrane, Yilgarn Craton.||||||
75246|Swincer Dolerite|73596|6|Mentioned|p1170|Mesoarchean|Mesoarchean|Mount Sefton Greenstone Belt, Burtville Terrane.|2812 +/- 5 Ma.|||||
78625|Syenite Camp Granodiorite|66846|5|Briefly described|p558 Table 4|Orosirian|Orosirian|Age probably from U-Pb SHRIMP dating of zircon (see p547).|~1819 Ma|Of Syenite Camp suite.||||
78625|Syenite Camp Granodiorite|72437|5|Briefly described|p100|||Whole rock analyses are provided.||Syenite Camp Suite|||Foliated hornblende-biotite tonalite, foliated biotite monzogranite, biotite monzogranite.|
31897|Syenite Camp Suite|50437|6|Mentioned|p4.1|||Of the Sally Downs Supersuite. Geological Province: Kimberley Region.||||||
31897|Syenite Camp Suite|65359|6|Mentioned|p23|||Felsic Suite in the Kimberley region.||||||
31897|Syenite Camp Suite|68078|6|Mentioned|p23|||||||||
31897|Syenite Camp Suite|69099|5|Briefly described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Of Sally Downs Supersuite.|Includes Corrara Granite, Grimpy Monzogranite.|||
31897|Syenite Camp Suite|69165|6|Mentioned|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||||Includes Corrara Granite, Grimpy Monzogranite|||
31897|Syenite Camp Suite|69634|5|Briefly described|100k_interpgeop_lut.csv|||||Unit of Sally Downs Supersuite.|Includes Corrara Granite, Grimpy Monzogranite.|||
31897|Syenite Camp Suite|70154|6|Mentioned|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1817 Ma|Sally Downs Supersuite|Includes Corrara Granite, Grimpy Monzogranite|||
31897|Syenite Camp Suite|70812|4|Described|p8, p24, p29, p38|Orosirian|Orosirian|Lamboo Province, most commonly in the Central Zone although units occur throughout the whole length of the province. Interpreted to have formed over a west or northwest dipping subduction zone in the Halls Creek orogeny. Not considered prospecite for REE.|c. 1835-1805 Ma|Sally Downs Supersuite|||Biotite-hornblende granodiorite, tonalite and monzogranite.|
31897|Syenite Camp Suite|70851|5|Briefly described|p5|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province. This unit has geochemistry indicative of crustally derived melts.||Sally Downs Supersuite|||Granitic rocks.|
31897|Syenite Camp Suite|71113|5|Briefly described|p101|Orosirian|Orosirian|Geological province: Central Zone, Lamboo Province, Halls Creek Orogen. Formed in a subduction zone setting.|>1820 Ma|Unit of Sally Downs Supersuite.||||
31897|Syenite Camp Suite|71140|6|Mentioned|p101|Orosirian|Orosirian|Lamboo Province, Halls Creek Orogen. Probably formed in a subduction zone setting.|>1820 Ma.|Sally Downs Supersuite.||||
31897|Syenite Camp Suite|71267|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma).||Unit of Sally Downs Supersuite.|Includes Corrara Granite.|||
34041|Sylvania Dyke Swarm|22475|4|Described|p495, Fig.1|Archean|Archean|See also p497, Figure 6, Table 1||||||07-NOV-08
34041|Sylvania Dyke Swarm|71803|6|Mentioned|p368||||2747+/- 4 Ma|||||
35246|Tabba Tabba Leucogranite|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
35246|Tabba Tabba Leucogranite|24110|5|Briefly described|Plate 1|Archean|Archean|Belongs to Pippingarra Granitoid Complex.  Geological Province: Pilbara Craton||||||07-NOV-08
35246|Tabba Tabba Leucogranite|24166|4|Described|p17|||Of the Pippingarra Granitoid Complex.||||||25-JUL-07
35246|Tabba Tabba Leucogranite|24193|5|Briefly described|p875 Fig.2|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
35246|Tabba Tabba Leucogranite|24327|5|Briefly described|Map Legend|Archean|Archean|Of the Pippingarra Granitoid Complex. Fine- to medium-grained biotite (-muscovite) granite.  Age: c.2940Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
35246|Tabba Tabba Leucogranite|24349|5|Briefly described|Map legend|Archean|Archean|Of the Pippingarra Granitoid Complex.  Age: c.2940Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
35246|Tabba Tabba Leucogranite|63420|5|Briefly described|Map legend|Archean|Archean|Of Split Rock Supersuite. Geological Province: Pilbara Craton. Biotite(-muscovite) granite; seriate to equigranular; fine- to medium-grained, massive to weakly foliated and metamorphosed.||||||07-NOV-08
35246|Tabba Tabba Leucogranite|63441|5|Briefly described|p11 Tb. 2|Archean|Archean|Of Sisters Supersuite. Geological province: Pilbara Craton.||||||07-FEB-11
35246|Tabba Tabba Leucogranite|68283|5|Briefly described|Map Legend|Archean|Archean|Pilbara Craton.||Of the Split Rock Supersuite.|||Biotite(-muscovite) granite; seriate to equigranular; fine to medium grained, massive to weakly foliated and metamorphosed.|23-SEP-13
35246|Tabba Tabba Leucogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Biotite(--muscovite) granite; seriate to equigranular; fine to medium grained; massive to weakly foliated and metamorphosed.|
35246|Tabba Tabba Leucogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; Split Rock Supersuite Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|2851-2831 Ma (inferred)|Unit of Split Rock Supersuite.|||Biotite(-muscovite) granite; seriate to equigranular; fine to medium grained; massive to weakly foliated and metamorphosed|
35246|Tabba Tabba Leucogranite|70775|5|Briefly described|p71, p81|||Mallina Basin. May be correlated with the Split Rock Supersuite, however it should be noted that geochronology is required to test this.||Split Rock Supersuite||Intrudes the Mallina Formation.|Biotite-muscovite granite that is massive to weakly foliated with seriate to equigranular texture.|
35246|Tabba Tabba Leucogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
35246|Tabba Tabba Leucogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Biotite(-muscovite) granite; seriate to equigranular; fine to medium grained; massive to weakly foliated and metamorphosed.|
32210|Table Top Formation|23416|5|Briefly described|Map Legend|Archean|Archean|Of Coonterunah Group, Pilbara Craton||||||07-NOV-08
32210|Table Top Formation|23755|4|Described|p18|Archean|Archean|See also page 17 Table 1. Of Coonterunah Group.||||||07-NOV-08
32210|Table Top Formation|23783|5|Briefly described|p10 Fig. 5|Archean|Archean|Of Coonterunah Group.||||||07-NOV-08
32210|Table Top Formation|23813|5|Briefly described|p91 Tb. 1|Archean|Archean|Of the Coonterunnah Group.  Age: c.3.51Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.||||||07-NOV-08
32210|Table Top Formation|24025|4|Described|p9 Tb. 1|Archean|Archean|Of Coonterunah Group. Basalt, local komatiitic basalt. Max. thickness: 2500m. Geological Province: Pilbara Craton.||||||11-APR-13
32210|Table Top Formation|24166|4|Described|p9|Archean|Archean|Of Coonterunah Group.||||||07-NOV-08
32210|Table Top Formation|24184|5|Briefly described|p699 Fig.3|Archean|Archean|Overlying Unit: Coucal Formation. Geological Province: Pilbara Craton. Age: <3515Ma||||||07-NOV-08
32210|Table Top Formation|24327|5|Briefly described|Map Legend|Archean|Archean|Fine to medium-grained amphibolite. Parent: Coonterunah Group. Age: c. 3515 Ma. Geological Province: Pilbara Craton.||||||16-APR-13
32210|Table Top Formation|24349|5|Briefly described|Map legend|Archean|Archean|Of Coonterunah Group. Age: c.3515 Ma. Geological Province: Pilbara Craton||||||16-APR-13
32210|Table Top Formation|24531|5|Briefly described|p5 Tb. 1|Archean|Archean|Of the Coonterunah Group (Pilbara Supergroup).  Geological Province: Pilbara Craton.||||||07-NOV-08
32210|Table Top Formation|24550|5|Briefly described|p31 Tb. 3.1|Archean|Archean|Of the Coonterunah Group. Basalt, komatiite. Geological Province: Pilbara Craton.||||||07-FEB-11
32210|Table Top Formation|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Of the Talga Talga Subgroup (Warrawoona Group). Basalt, local komatiitic basalt.||||||07-FEB-11
32210|Table Top Formation|50379|5|Briefly described|Map Legend|Archean|Archean|Of Coonterunah Group (Pilbara Supergroup). Geological Province: Pilbara Craton.||||||07-NOV-08
32210|Table Top Formation|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Geological Province: eastern Pilbara Craton.||||||07-NOV-08
32210|Table Top Formation|61266|4|Described|p56-57 Fig.1|Archean|Archean|Of the Coonterunah Group. Overlain by the Coucal Formation. Thickness: ~2500m. Dominantly tholeiitic basalt, with thin, cherty interbeds, and minor high-Mg and komatiitic basalt. Geological Province: Pilbara Craton. See also p58 Tb.1.||||||07-NOV-08
32210|Table Top Formation|61579|5|Briefly described|p58 Fig. 2|Archean|Archean|Of the Coonterunah Group.||||||07-NOV-08
32210|Table Top Formation|63420|5|Briefly described|Map legend|Archean|Archean|Of Coonterunah Subgroup (Warrawoona Gp, Pilbara Supergp). Geol.Prov: Pilbara Craton. Amphibole, minor mafic schist, locally silicified. Dominantly qtz- and feldspar-porphyritic rhyolite intrusive rock, subordinate felsic tuffaceous sst and qtz arenite.||||||07-NOV-08
32210|Table Top Formation|63441|5|Briefly described|p4 Tb. 1|Archean|Archean|Of Coonterunah Subgroup (Warrawoona Group, Pilbara Supergroup).||||||07-FEB-11
32210|Table Top Formation|63538|4|Described|p8, p11, p13, p19, p6 Fig. 3|Archean|Archean|Of Coonterunah Subgroup. Overlain by Coucal Formation. Geological Province: Pilbara Craton. Tholeiitic basalt pile. Seen also as Tabletop Formation (misspelt).||||||19-APR-13
32210|Table Top Formation|64328|5|Briefly described|p56 Tb. 1|||Of the Coonterunah Group. Basalt.||||||07-FEB-11
32210|Table Top Formation|64405|5|Briefly described|p4|Archean|Archean|Name inferred from Table Top only in Figure 3. Of the Warrawoona Group (De Grey Supergroup).||||||07-FEB-11
32210|Table Top Formation|66664|6|Mentioned|p7.||||||||Metabasalt.|
32210|Table Top Formation|66745|5|Briefly described|p54 Fig.4.|Paleoarchean|Paleoarchean|||Unit in Coonterunah Subgroup.||Is overlain by Coucal Formation.|Basalt; chert.|
32210|Table Top Formation|67197|5|Briefly described|p4-5|Paleoarchean|Paleoarchean|East Pilbara Terrane. Intruded by granitic rocks aged 3467 Ma.|>3515 Ma.|Coonterunah Subgroup.||||
32210|Table Top Formation|67201|5|Briefly described|p7 Fig.4, p12 Tb.1|||In northern Pilbara Craton, East Pilbara Terrane.|c. 3525|Coonterunah Subgroup||||
32210|Table Top Formation|67269|5|Briefly described|p6 Fig.3|Paleoarchean|Paleoarchean|||Coonterunah Subgroup.|||Basalt.|
32210|Table Top Formation|67270|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Coonterunah Subgroup.||||
32210|Table Top Formation|67668|6|Mentioned|Fig. 2; p. 153||Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Coonterunah Subgroup of the Warrawoona Group||Underlies the Coucal Formation.|Mafic volcanic rocks.|17-SEP-14
32210|Table Top Formation|68035|5|Briefly described|p288 Fig 4|Paleoarchean||Warrawoona Group, Pilbara Supergroup, East Pilbara Terrane.||Of Coonterunah Subgroup||Intruded by granitic rocks. Overlain by Coucal Formation.|Basalt.|
32210|Table Top Formation|68280|6|Mentioned|p4|||||Coonterunah Subgroup||Overlain by Coucal Formation||
32210|Table Top Formation|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. The 4 facies are mapped separately.||Of the Coonterunah Subgroup.|||Amphibolite; metamorphosed mafic volcanic and intrusive rocks; locally schistose; strongly sheared amphibolite schist; metachert; metamorphosed jaspilitic chert.|23-SEP-13
32210|Table Top Formation|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Age inferred from parent unit.||Of the Coonterunah Subgroup.|||Amphibolite; metamorphosed mafic volcanic and intrusive rocks; locally schistose.|19-JUN-14
32210|Table Top Formation|68284|5|Briefly described|p7|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Coonterunah Subgroup.||Is overlain by Coucal Formation.||
32210|Table Top Formation|69013|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane. Includes 2 unnamed sub-units mapped separately.||Of the Coonterunah Subgroup.|||Amphibolite; metamorphosed mafic volcanic and intrusive rocks; locally schistose.|30-APR-14
32210|Table Top Formation|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. ||Of the Coonterunah Subgroup.|||Amphibolite; metamorphosed mafic volcanic and intrusive rocks; locally schistose.|02-MAY-14
32210|Table Top Formation|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Coonterunah Subgroup|||Banded iron formation, interleaved mafic or ultramafic schist, metadolerite and amphibolite schist, Amphibolite; metamorphosed mafic volcanic and intrusive rocks; locally schistose.|
32210|Table Top Formation|69301|4|Described|p5 Fig.3, p9 Tb.1|||Pilbara Craton. East Pilbara Terrane. East Strelley Greenstone Belt. This is the oldest recognized formation of Pilbara Supergroup.|>3525 Ma|Coonterunah Subgroup||Extensively intruded by granites of Carlindi Granitic Complex.|Basalt.|
32210|Table Top Formation|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.|3515 Ma (inferred)|Unit of Coonterunah Subgroup.|||Amphibolite and amphibolite schist; metamorphosed mafic volcanic and intrusive rocks; locally schistose; metadolerite; banded iron-formation and interleaved mafic or ultramafic schist.|
32210|Table Top Formation|70022|6|Mentioned|p115|||East Pilbara Terrane.||Coonterunah Subgroup.||||
32210|Table Top Formation|70775|5|Briefly described|p12|Paleoarchean|Paleoarchean|East Pilbara.|c. 3525 Ma|Warrawoona Group||Overlain by the Coucal Formation.||
32210|Table Top Formation|70884|5|Briefly described|p123|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Coonterunah Subgroup.||Overlain by Coucal Formation.||
32210|Table Top Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Warrawoona  Large Igneous Province.||Coonterunah Subgroup|||Amphibolite; metamorphosed mafic volcanic and intrusive rocks; locally schistose.|
32210|Table Top Formation|72064|5|Briefly described|p66|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawoona Group.||Lowermost unit of Warawoona Group. Overlain by Coucal Formation.||
32210|Table Top Formation|72251|5|Briefly described|p54|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unt of Coonterunah Subgroup.||Lwoermost unit of Coonterunah Group. Overlain by Coucal Formation.||
32210|Table Top Formation|72668|5|Briefly described|p4-8. p10-11|||East Pilbara Terrane.||Coonterunah Subgroup||Overlain by the Coucal Formation.||14-JAN-22
32210|Table Top Formation|73598|6|Mentioned|p1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Coonterunah Subgroup.||Is overlain by Coucal Formation.||
80128|Table Well Monzogranite|71212|5|Briefly described|p80-82, p90, p72, 248|||Yilgarn Craton. Named for the Table Well. See also App C.|||||Meso-melanocratic, biotite rich granodiorites to leucocratic K-feldspar rich granites.|26-SEP-17
80128|Table Well Monzogranite|73151|6|Mentioned|p3-4|Neoarchean|Neoarchean|Yilgarn Craton. Age from Black et al., (2002).|2665 +/- 4 Ma||||Granitic rocks.|
36912|Tabletop granitoid complex|23602|5|Briefly described|p2 Fig 1|||||||||
36912|Tabletop granitoid complex|23742|5|Briefly described|p2 Fig 1||Mesoproterozoic|Informal name.||||||
36912|Tabletop granitoid complex|64943|6|Mentioned|p3 Fig. 1|Mesoproterozoic|Mesoproterozoic|||||||
74837|Taincrow Monzogranite|64891|5|Briefly described|p37 Fig. 2, p52-53 Tb. 1|Archean|Archean|Of Walganna Suite (Bald Rock Supersuite). Age: c. 2625Ma. Geological province: Murchison Domain. Monzogranite to syenogranite; post-tectonic.||||||07-FEB-11
74837|Taincrow Monzogranite|67129|6|Mentioned|p19 fig 20|Archean|Archean|Murchison Domain, Youanmi Terrane.||Bald Rock Supersuite|||Post-tectonic monzogranite.|07-SEP-17
74837|Taincrow Monzogranite|69583|5|Briefly described|p49, p52|Neoarchean|Neoarchean|Murchison Domain. See also Taincrow Granite (p43).||Walganna Suite.||||
74837|Taincrow Monzogranite|69584|5|Briefly described|p5 Fig.2|Neoarchean|Neoarchean|||Walganna Suite|||Monzogranite.|
74837|Taincrow Monzogranite|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Walganna Suite.||||
74837|Taincrow Monzogranite|70030|5|Briefly described|p191|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton.||Unit of Bald Rock Supersuite.||||
74837|Taincrow Monzogranite|70830|6|Mentioned|p8|||Murchison Domain. ||||||
82964|Talbot Formation|73238|5|Briefly described|p21|||White Flag Lake, Gidji area, Eastern Goldfields Terrane. Deformation structures briefly described.||||||
82964|Talbot Formation|73596|6|Mentioned|p1159-1160, 1162|Neoarchean|Neoarchean|Kalgoorlie-Kambalda area.|c.2690-2680 Ma.|Black Flag Group.||Overlies Paringa Basalt (Hannans Subgroup). Is overlain by White Flag Formation.||
31875|Taliwanya Formation|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Throssell Group, Yeneena Basin.||||||
31875|Taliwanya Formation|23602|5|Briefly described|p15|||Of Throssell Group. Underlying unit Rudall Complex.||||||
31875|Taliwanya Formation|23742|4|Described|p6||Mesoproterozoic|Of Throssell Group. Overlying unit Pungkuli Formation. Max. thickness: 170 m.||||||
31875|Taliwanya Formation|23760|4|Described|p22|Neoproterozoic|Mesoproterozoic|Of Throssell Group. Geological Province: Yeneena Basin. Max. thickness: 170 m.||||||
31875|Taliwanya Formation|24594|5|Briefly described|p601|Neoproterozoic|Mesoproterozoic|Of the Throssell Group.  Siliciclastic unit.   Geological Province: Yeneena Basin (Paterson Orogen).||||||09-JUL-13
31875|Taliwanya Formation|43848|5|Briefly described|Map Legend||Proterozoic|Of Throssell Group, Yeneena Supergroup.||||||
31875|Taliwanya Formation|43849|5|Briefly described|Map Legend||Proterozoic|Of Throssell Group.||||||
31875|Taliwanya Formation|62453|3|Fully described|p68|Cryogenian|Cryogenian|Of the Throssell Range Group. Paterson Orogen. Underlies Pungkuli Formation, Coolbro Sandstone and Broadhurst Formation. Thickness: 170m. Sandstone, conglomerate, wacke, siltstone and shale. ||||||
31875|Taliwanya Formation|64580|4|Described|map legend|Neoproterozoic|Mesoproterozoic|Fine- to medium-grained  arkose to arkosic sandstone, well bedded; with local thick beds of polymictic conglomerate and rare thin interbeds of lithic wacke, siltstone, and shale.||||||15-DEC-08
31875|Taliwanya Formation|65403|4|Described|p13.|||New name. Named after a local track. Occurs on both sides of McKay Fault. Thickness to 170 m. Interpreted as channel-fill deposit.||Basal unit in Throssell Group in Connaughton area..||Unconformably overlies Rudall Complex. Is overlain conformably by Pungkuli Formation.|Polymictic conglomerate and arkosic sandstone with rare heavy-mineral bands; thin interbeds of fine-grained lithic wacke, siltstone and shale.|29-SEP-15
31875|Taliwanya Formation|65454|4|Described|p7-8, p10-11, p30 Fig.A1b|Cryogenian|Cryogenian|Yeneena Basin. Of basal Throssell Range Group. Arkose, arkosic sandstone and siltstone. Medium- to coarse-grained. Unconformably overlying basement.||||||
31875|Taliwanya Formation|67182|6|Mentioned|p677 Fig.2|Neoproterozoic|Neoproterozoic|||||||
31875|Taliwanya Formation|67202|4|Described|p58, p65, p157, p219, p229, p231, p233|Neoproterozoic|Neoproterozoic|See also p235, p237-238, p241, p243, p247, p272. Formally defined by Bagas and Smithies (1998). Up to 170m thick.||Throssell Range Group.||Unconformably overlies Rudall Complex. Is overlain conformably by Pungkuli Formation. May correlate with Coolbro Sandstone.|Polymictic conglomerate, arkosic sandstone, coarse sandstone with rare heavy-mineral bands; minor fine-grained lithic wacke, siltstone and shale.|15-FEB-18
31875|Taliwanya Formation|67430|6|Mentioned|p22|||Paterson Province.||||||
31875|Taliwanya Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||arkose, sandstone|
31875|Taliwanya Formation|72034|5|Briefly described|500k_interpgeop16_lut|Cryogenian|Tonian|Yeneena Basin. Assignment to Throssell Range Group uncertain.||Throssell Range Group.|||Arkose to arkosic sandstone, with local thick beds of polymictic conglomerate and rare thin interbeds of lithic wacke, siltstone, and shale; assignment to Throssell Range Group uncertain.|
26923|Tallering Formation|29688|4|Described|p43|||||||||
26923|Tallering Formation|29690|5|Briefly described|p8|||||||||
26923|Tallering Formation|30949|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
26923|Tallering Formation|32337|6|Mentioned|p12|||||||||
26923|Tallering Formation|40815|4|Described|p277|||||||||
74681|Tambina Granitic Complex|64405|6|Mentioned|p16|||Also informally referred to as the Tambina greenstone complex. Contains no Strelley Pool Formation rocks, as do many other greenstone belts in the East Pilbara Terrane - 11 out of 20 have identified Strelley Pool Formation within them.||||||07-FEB-11
74681|Tambina Granitic Complex|64580|4|Described|map legend||Paleoarchean|Undivided granitoid rock ; well foliated.||||||05-NOV-08
68742|Tambina Supersuite|61253|5|Briefly described|p56, p52 Fig. 2, p58|Archean|Archean|Has inclusions of Sisters Supersuite material within its monzogranite. Age: 3435-3420Ma; age also given as 3.44 to 3.42Ga.  Geological Province: eastern Pilbara Craton.  See also p54-55 Fig. 3.||||||07-NOV-08
68742|Tambina Supersuite|63417|5|Briefly described|Map legend|Archean|Archean|Includes Lady Adelaide Orthogneiss and Fig Tree Gneiss. Age: c.3429Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
68742|Tambina Supersuite|63420|5|Briefly described|Map legend|Archean|Archean|Includes Wilson Well Gneiss and two unnamed metatonalite units.  Age: c.3420Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
68742|Tambina Supersuite|63441|4|Described|p35, p7 Tb. 2, p30|Archean|Archean|Its granitic rocks(sodic) outcrop in both Shaw and Mount Edgar Granitic Complexes (Abyssinia Well Orthogneiss, and Fig Tree Gneiss +Lady Adelaide Orthogneiss respectively). Age:3450-3420Ma. Geol.prov:East Pilbara Terrane.See also p31 Fig. 10, p33 Fig. 12.||||||07-FEB-11
68742|Tambina Supersuite|63538|6|Mentioned|p6 Fig. 3|Archean|Archean|Geological Province: Pilbara Craton.||||||19-APR-13
68742|Tambina Supersuite|64405|5|Briefly described|p19, p21|Archean|Archean|Age: c.3450-3420Ma. Consists of granitic rocks broadly contemporaneous with Panorama Formation. Geological province: East Pilbara Terrane.||||||07-FEB-11
68742|Tambina Supersuite|64621|5|Briefly described|Map legend|Archean|Archean|Age: 3448-3428Ma. Includes Bookargemoona Tonalite and Fig Tree Gneiss and unnamed units of interlayered granitic gneiss and mafic amphibolite, and leucocratic monzogranite.||||||07-NOV-08
68742|Tambina Supersuite|64654|5|Briefly described|Map Legend|Archaean|Archaean|Age: 3435-3425Ma. Geological Province: Pilbara Craton. Equigranular, leucocratic granodiorite; generally medium grained; predominantly foliated.||||||
68742|Tambina Supersuite|64657|5|Briefly described|Map Legend|Archaean|Archaean|Age: 3435-3425Ma. Geological Province: Pilbara Craton. Equigranular, leucocratic granodiorite; generally medium grained; predominantly foliated.||||||26-NOV-08
68742|Tambina Supersuite|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|||Includes Fig Tree Gneiss and Lady Adelaide Orthogneiss.|||
68742|Tambina Supersuite|65827|3|Fully described|p1, p6 Tb.2, p9 Fig 3, p15, p20, p22|Paleoarchean|Paleoarchean|3450-3420 Ma. Of Mount Edgar Granitic Complex. Includes Lady Adelaide Orthogneiss, Fig Tree Gneiss. Lies along the margins of Mount Edgar Granitic Complex. Intruded by Emu Pool Supersuite. Banded gneiss and gneissic granitic rocks.||||||
68742|Tambina Supersuite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Includes Bookargemoona Tonalite, Petroglyph Gneiss, Fig Tree Gneiss, Yallingarrintha Tonalite, and an unnamed unit of metatonalite to metasyenogranite with local greenstone and orthogneiss xenoliths. ||||||
68742|Tambina Supersuite|66217|4|Described|p5, p6, p10, p12, p14, p15, pp27-28.|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Predominantly sodic; derived from melting of basaltic protoliths. Emplaced as sheeted sill complex in greenstones contemporaneously with Warrawoona Group volcanism.|3450-3420 Ma (Van Kranendonk et al. 2006a).|Unit in Muccan, Shaw and Mount Edgar Granitic Complexes, and Carlindi Granitoid Complex.|Includes Wilson Well Gneiss.|Intrudes Pilbara Supergroup.|Foliated tonalite-trondhjemite-granodiorite; biotite-hornblende leucogranite; gneiss.|
68742|Tambina Supersuite|67201|6|Mentioned|p7 Fig.6|||East Pilbara Terrane.||||||
68742|Tambina Supersuite|67269|5|Briefly described|p5|Paleoarchean|Paleoarchean||||||Tonalite and granodiorite; includes dykes.|
68742|Tambina Supersuite|68035|5|Briefly described|p286 Fig 3|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Associated with upper Warrawoona Group.|3.46 - 3.42 Ga|||||
68742|Tambina Supersuite|68280|6|Mentioned|p3|Paleoarchean|Paleoarchean||3460-3420 Ma|||||
68742|Tambina Supersuite|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Detailed lithology discussed in map legend; the 4 facies are mapped separately.|||Includes Wilson Well Gneiss.||Metagranodiorite with amphibolite xenoliths; foliated leucocratic metamonzogranite and local diatexite, as sheets; meta hornblende monzogranite and metagranodiorite; migmatitic tonalitic orthogneiss and schlieric hornblende granodiorite.|23-SEP-13
68742|Tambina Supersuite|68282|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. 12 facies are mapped separately.|||Includes Petroglyph Gneiss.|||
68742|Tambina Supersuite|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. U-Pb SHRIMP age from Van Kranendonk (unpublished).|c. 3420 Ma||Includes Wilson Well Gneiss.||Metatonalite, grades to metagranodiorite; tonalitic orthogneiss.|19-JUN-14
68742|Tambina Supersuite|69012|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane. Three unnamed sub-units are also mapped separately.|3451-3427 Ma (Zegers, 1996)||Includes the Bookargemoona Tonalite.||Biotite tonalite, hornblende monzogranite and metagranodiorite, leucocratic monzogranite; all metamorphosed.|28-APR-14
68742|Tambina Supersuite|69013|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane.|||Includes Yallingarrintha Tonalite and Petroglyph Gneiss.||Includes meta-biotite-hornblende tonalite to metagranodiorite; tonalitic orthogneiss with sheeted pegmatitic granite veins and local white leucogranite; foliated to gneissic granitic rock with abundant mafic and ultramafic xenoliths.|29-APR-14
68742|Tambina Supersuite|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Also includes 3 unnamed sub-units, mapped separately. See map legend for a detailed lithological description.|< 3459 Ma (Thorpe et al. 2002)||Includes Wilson Well Gneiss, Petroglyph Gneiss, and North Pole Monzogranite.||Includes leucocratic monzogranite; orthogneiss; tonalitic orthogneiss and schlieric hornblende granodiorite; biotite monzogranite.|02-MAY-14
68742|Tambina Supersuite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean||||Includes Yallingarrintha Tonalite, Bookargemoona Tonalite, Petroglyph Gneiss, Fig Tree Gneiss, Lady Adelaide Orthogneiss, Wilson Well Gneiss, North Pole Monzogranite||Metatonalite, metaquartz diorite, metagranodiorite,metamonzogranite, monzogranite. Metatonalite with abundant greenstone xenoliths; massive to strongly foliated. Metatonalite to metagranodiorite, leucocratic orthogneiss, biotite granite orthogneiss.|
68742|Tambina Supersuite|69301|6|Mentioned|p5 Fig.3|||Pilbara Craton. East Pilbara Terrane. Pilbara Supergroup successions include thick felsic volcanic formations, each contemporaneous with the four granitic supersuites. i.e. Panorama Formation and Tambina Supersuite.||||||
68742|Tambina Supersuite|69566|5|Briefly described|p236-237, 248|||Mount Edgar Granitoid Complex, East Pilbara Granite-Greenstone Terrane.|3448-3424 Ma.||Fig Tree Gneiss, Lady Adelaide Orthogneiss.||Voluminous TTG magmatism; gneisses.|
68742|Tambina Supersuite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv.|3459-3410 Ma (inferred)||Includes Bookargemoona Tonalite, Fig Tree Gneiss, Lady Adelaide Orthogneiss, North Pole Monzogranite, Petroglyph Gneiss, Wilson Well Gneiss, Yallingarrintha Tonalite.||Biotite granitic orthogneiss, leucocratic metagranodiorite and monzogranite, metagranodiorite, metatonalite, metamorphosed biotite-granodiorite and hornblende-monzogranite.|
68742|Tambina Supersuite|70022|6|Mentioned|p115-116|||East Pilbara Terrane.|3.66-3.41 Ga.||Warrawagine Granitic Complex.|||
68742|Tambina Supersuite|70775|6|Mentioned|p69||||c. 3430 Ma|||||
68742|Tambina Supersuite|70884|5|Briefly described|p122-123,134-135|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Contains ~3.41 Ga metamorphic zircons withindomes (U-Pb SHRIMP; Nelson, 1999), and  3.44 Ga metamorphic monazite within greenstone metasedimentary rocks (U-Th-Pb SHRIMP; Francois et al., 2014) associated with Muccan Granitic Complex emplacement and crustal uplift.|3.45-3.42 Ga|||||
68742|Tambina Supersuite|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||granodiorite, granite, felsic gneiss, pegmatite|
68742|Tambina Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Includes 6 named and 2 unnamed units.|Max age 3451+/-1 Ma, min 3416 +/-8 Ma.||Includes Fig Tree Gneiss, Wilson Well Gneiss, Petroglyph Gneiss, Bookargemoona Tonalite, North Pole Monzogranite, Lady Adelaide Orthogneiss.|Tambina Supersuite tonalite includsions in Nandingarra Granodiorite.|Metatonalite/metagranodiorite; gneissic to massive; local leucocratic monzogranite. Metatonalite w abundant greenstone xenoliths; massive to strongly foliated. Metagranodiorite w amphibolite xenoliths ; equigranular, mesocratic to melanocratic.|
68742|Tambina Supersuite|72064|6|Mentioned|p79|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Overlaps in age with Paleoarchean zircons found in the Strelley Pool Formation.|3.45-3.42 Ga|||||
68742|Tambina Supersuite|72251|5|Briefly described|p52-55,63,65,67|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Comtemporaneous with rhyolitic Panorama Formation (Van Kranendonk et al., 2006). A major component of the Shaw Granitic Complex, and interpreted to be derived from melting of Callina Supersuite protoliths (Pawley et al., 2004). Granitic supersuite with Nd model age of ~4.1-3.4 Ga (Smithies et al., 2003, 2007; Champion, 2013). Contains two gneissic tonalitic enclaves dated at c. 3.59-3.58 Ga, which may be attributed to the Mount Webber Gabbro.|3.45-3.42 Ga|||||
68742|Tambina Supersuite|72668|5|Briefly described|p4, p9, p11, p13, p17-19, p25|||Comagmatic with the eruption of the Panorama Formation. Represents melt derived from Callina Supersuite protoliths.|c. 3450-3420 Ma||||Contains widespread leucogranite.|14-JAN-22
68742|Tambina Supersuite|73598|6|Mentioned|p1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.||||||
39604|Tambourah Monzogranite|24531|5|Briefly described|p8-9 Fig. 3|Archean|Archean|Of the Yule Granitoid Complex.||||||07-NOV-08
39604|Tambourah Monzogranite|24532|5|Briefly described|Map legend|Archean|Archean|Of the Yule Granitoid Complex.||||||07-NOV-08
39604|Tambourah Monzogranite|24554|4|Described|p5 Tb.1, p8|Archean|Archean|Of the Yule Granitoid Complex. Age: c. 2945-2930 Ma. Geological Province: East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
39604|Tambourah Monzogranite|50146|5|Briefly described|Map Legend|Archean|Archean|Of the Yule Granitoid Complex. Geological Province: Pilbara Craton. Dominantly course-grained syenogranite and pegmatite; locally abundant xenoliths of strongly foliated biotite granodiorite and granitoid gneiss.||||||07-NOV-08
39604|Tambourah Monzogranite|63441|5|Briefly described|p7 Tb. 2, p11 Tb. 2|Archean|Archean|Of the Sisters Supersuite. Supersedes Tambourah Granodiorite. Geological Province: Pilbara Craton. (Note: incorrect grouping in Tambina Suite, page 7)||||||15-APR-13
39604|Tambourah Monzogranite|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Sisters Supersuite. Geological Province: Pilbara Craton. Pegmatite and coarse-grained syenogranite in fine- to medium-grained, weakly foliated, biotite granodiorite.||||||
39604|Tambourah Monzogranite|66108|5|Briefly described|Map legend|Neoarchean|Neoarchean|Unit in Split Rock Supersuite. Pegmatitic to coarse-grained granite; generally as irregular patches in foliated biotite granodiorite (?Kavir Granodiorite).||||||
39604|Tambourah Monzogranite|68282|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.||Of the Split Rock Supersuite|||Pegmatitic to coarse-grained granite; generally as irregular patches in foliated biotite granodiorite.|
39604|Tambourah Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Pegmatitic to coarse-grained granite, generally as irregular patches in foliated biotite granodiorite (?Kavir Granodiorite). Pegmatitic leucogranite in strongly foliated biotite metagranodiorite and gneissic metatonalite.|
39604|Tambourah Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; Split Rock Supersuite Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|2851-2831 Ma (inferred)|Unit of Split Rock Supersuite.|||Pegmatitic leucogranite in strongly foliated biotite metagranodiorite and gneissic metatonalite; pegmatitic to coarse-grained granite.|
39604|Tambourah Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||pegmatite, syenogranite, granodiorite, monzogranite|
39604|Tambourah Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Pegmatitic to coarse-grained granite, generally as irregular patches in foliated biotite granodiorite (?Kavir granodiorite).|
37095|Tangadee Rhyolite|23485|5|Briefly described|p30|Statherian|Statherian|Of Bangemall Supergroup.  Age: c.1640Ma (SHRIMP U-Pb zircon).||||||
37095|Tangadee Rhyolite|23525|6|Mentioned|p29|||Parent: Edmund Group. Geological Province: Edmund Basin.||||||08-SEP-08
37095|Tangadee Rhyolite|23744|6|Mentioned|p24|||||||||
37095|Tangadee Rhyolite|23747|6|Mentioned|p4|||||||||
37095|Tangadee Rhyolite|64287|6|Mentioned|p33 Tb. 1|||||||||07-FEB-11
37095|Tangadee Rhyolite|66241|4|Described|pp1-4, pp6-9, pp11-12, p15, pp28-29. |Ectasian|Ectasian|Interbedded with lower Kiangi Creek Formation sandstone and conglomerate, east of Abra deposit. The lithology is described in detail. Gee et al. (1976) record an alteration event at 1098 +/- 42 Ma.  Contains xenotime with oscillatory-zoned cores dated 1235 +/- 19 Ma (?crystallisation), with unzoned rims dated 1030 +/- 40 Ma (?later hydrothermal event).|c.1235 Ma.|Unit in Kiangi Creek Formation.|||Coherent rhyolite and lapilli-bearing felsic volcaniclastic rocks.|
37095|Tangadee Rhyolite|69003|6|Mentioned|p4|||Capricorn Orogen.||||||
37095|Tangadee Rhyolite|69166|4|Described|geologyp_lut.csv|Mesoproterozoic|Paleoproterozoic|||Edmund Group|||Felsic volcaniclastic sandstone and siltstone; abundant accretionary lapilli locally. Massive or flow banded rhyolite that is locally porphyritic.|
37095|Tangadee Rhyolite|70019|5|Briefly described|p92-94||Paleoproterozoic|Geological province: Gascoyne Province, Capricorn Orogen. Rb-Sr date of 1098+\-42 Ma from Gee et al., 1976 was intepreted as a post-emplacement alteration age. U-Pb zircon ages from Nelson 1995 yielded maximum depositional age of 1638+\-14 Ma.|<1638+\-14 Ma.||||Ccoherent lava flows and tuffaceous layers.|
37095|Tangadee Rhyolite|70795|4|Described|100k_geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Also 100k_interpgeop_lut.csv, West Australian Craton, Edmund Basin|1590-1517 Ma|Kiangi Creek Formation|||Felsic volcaniclastic sandstone and siltstone, massive or flow banded rhyolite, locally porphyritic.|31-JAN-18
37095|Tangadee Rhyolite|70814|5|Briefly described|p12, p47|Ectasian|Ectasian|Edmund Basin. See also Tangadee Rhyolite Member. A metamorphic age of c. 1235 Ma is given from Rasmussen et al., 2010.||Kiangi Creek Formation|||Felsic volcanic rocks.|31-JAN-18
80325|Tangadee Rhyolite Member|70814|5|Briefly described|p9, p12, p18, p39, 47|||Edmund Basin.[Intended to supersede Tangadee Rhyolite, or more clearly explain its member status]. Re-Os dates from hydrothermal xenotime  c.1235 Ma mentioned p18, 39.||Kiangi Creek Formation|||Felsic volcanic rocks.|22-SEP-18
36895|Tanguin Member|23570|4|Described|p151|Archean|Archean|Of Hardey Formation.   Overlain by Warroo Hill Member; underlain by Warri Warri Member.   Geological Province: Pilbara Craton||||||07-NOV-08
36895|Tanguin Member|23594|5|Briefly described|p9 Fig 6|Archean|Archean|Of Hardey Formation. Hamersley Basin.||||||07-NOV-08
36895|Tanguin Member|23746|5|Briefly described|p16|Archean|Archean|Of Hardey Formation. Geological Province: Hamersley Basin.||||||07-NOV-08
36895|Tanguin Member|67202|5|Briefly described|p236|Archean|Archean|Potential trap for uranium.||Hardey Formation|||Mixed felsic and mafic lavas (rhyolite and basalt) and tuffaceous sedimentary rocks.|15-FEB-18
36895|Tanguin Member|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Hardey Formation|||Mixed felsic (rhyolites) and mafic (basalts) lavas; minor volcaniclastic sedimentary rocks|
36895|Tanguin Member|69590|4|Described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Of Northeast Pilbara Sub-basin; Marble Bar Sub-basin, Fortescue Basin. Events: Pilbara Craton breakup.|2766-2749 Ma (inferred)|Unit of Hardey Formation.|||Mixed felsic and mafic lavas; basalt and rhyolite; minor volcaniclastic sedimentary rocks|
81035|Tank 44 Gneiss|70802|4|Described|250k_pre_mesozoic_interpgeop_lut.csv|Mesoproterozoic|Paleoproterozoic|Geological province: Biranup Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage II (1225-1140 Ma); Albany-Fraser Orogeny (1330-1140 Ma); Albany-Fraser Orogeny Stage I (1330-1260 Ma); Biranup Orogeny (1710-1620 Ma); Zanthus Event (1680-1675 Ma); Ngadju Event (1780-1760 Ma); Salmon Gums Event (1815-1800 Ma).|1800 Ma (inferred); 1209+\-5 Ma||||Interlayered mafic and quartzofeldspathic gneiss with abundant leucosomes, locally with garnet|
81035|Tank 44 Gneiss|71270|4|Described|500k_interpgeop16_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Kepa Kurl Booya Province, Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage II (1225 - 1140 Ma); Albany-Fraser Orogeny (1330 - 1140 Ma); Albany-Fraser Orogeny Stage I (1330 - 1260 Ma); Biranup Orogeny (1710 - 1620 Ma); Zanthus Event (1680 - 1675 Ma); Ngadju Event (1780 - 1760 Ma); Salmon Gums Event (1815 - 1800 Ma).|1800-1201 Ma (inferred)||||Interlayered mafic and quartzofeldspathic gneiss with abundant leucosomes, locally with garnet|
81035|Tank 44 Gneiss|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Paleoproterozoic|Biranup Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen.|Max age ~1800 Ma, Min age 1201+/-5 Ma.||||Interlayered mafic and quartzofeldspathic gneiss with abundant leucosomes, locally with garnet.|
26162|Tantabiddi Member|23726|5|Briefly described|p93 Fig 29|||Overlying unit Jurabi Member.||||||
26162|Tantabiddi Member|33593|2|Defined|p114|Holocene|Pleistocene|Pleistocene - Holocene||||||
26162|Tantabiddi Member|35796|6|Mentioned|p285|||||||||
26162|Tantabiddi Member|37016|6|Mentioned|Map legend|Holocene|Pleistocene|Pleistocene to Holocene.||||||
26162|Tantabiddi Member|38954|6|Mentioned|Table 1|||||||||
26162|Tantabiddi Member|39427|4|Described|Table 1|||||||||
26162|Tantabiddi Member|41271|3|Fully described|p194|||||||||
26162|Tantabiddi Member|41468|6|Mentioned|p1279|||||||||
26162|Tantabiddi Member|42116|6|Mentioned|Fig.28 P72|||||||||
26162|Tantabiddi Member|66125|5|Briefly described|p133 Fig.4, 136-137|||Ningaloo Reef area; onshore. Occupies the area between the present-day lagoon and the Tantabiddi Scarp. Detailed core log with photos.||Bundera Calcarenite.|||Lagoonal and reef facies underlie and crop out in the coastal zone of littoral and aeolian sandy deposits.|
73784|Tantalite Hill pegmatite|50542|5|Briefly described|p135|||Informal name. Consists of two main flat-lying pegmatite bodies, the southern body has a thickness of 5m and the northern body thickness is 25m.||||||07-FEB-11
32533|Tarakalu Member|24371|5|Briefly described|p209|Famennian|Famennian|Geological Province: Canning Basin.||||||10-NOV-08
32533|Tarakalu Member|64502|6|Mentioned|p785|||Of Napier Formation in Dingo Gap area.||||||10-NOV-08
32533|Tarakalu Member|66127|5|Briefly described|p63-64, p245 Fig.326, Plate 2. |Famennian|Famennian|Named after the Aboriginal name for Dingo Gap. Lower and middle parts of the unit are poorly exposed. Contains minor stromatolites and conodonts.||Unit in Napier Formation.|||Medium-grained quartz-feldspar sandstone; locally calcareous with interbeds of siltstone, calcarenite and breccia; with some allochthonous blocks of reef limestone.|
31872|Tarcunyah Group|22716|6|Mentioned|table4, p238|||Unconformably overlies Yeneena Basin. Also part of supersequence 1 of Centralian Superbasin||||||
31872|Tarcunyah Group|22816|5|Briefly described|p8 Table 1|||Savory Group||||||
31872|Tarcunyah Group|22907|6|Mentioned|39|||||||||
31872|Tarcunyah Group|23314|5|Briefly described|331 Fig.2|||||||||
31872|Tarcunyah Group|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Officer Basin.||||||
31872|Tarcunyah Group|23415|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Includes Eel Creek Formation.||||||07-JAN-08
31872|Tarcunyah Group|23575|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Overlying unit Savory Group.||||||
31872|Tarcunyah Group|23583|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
31872|Tarcunyah Group|23585|4|Described|p21|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
31872|Tarcunyah Group|23590|2|Defined|p10, p22 Appendix 2|Neoproterozoic|Neoproterozoic|Age: <830-c.600 Ma (poor age constraints). Overlain by Tchukardine Formation. Underlain by Throssell Group. Geological Province: Officer Basin. Max. thickness 4300 m.||||||22-JUL-09
31872|Tarcunyah Group|23594|4|Described|p21|Neoproterozoic|Neoproterozoic|Age: c.800 Ma. Underlain by Gregory Granitic Complex. Geological Province: Officer Basin.||||||25-JUL-07
31872|Tarcunyah Group|23602|5|Briefly described|p16|Neoproterozoic|Neoproterozoic|Age: c.800 Ma. Overlain by Savory Group.||||||25-JUL-07
31872|Tarcunyah Group|23729|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Paterson Orogen.||||||
31872|Tarcunyah Group|23730|4|Described|p10|Neoproterozoic|Neoproterozoic|Age: c830-700 Ma. Overlain by Tchukardine Formation. Underlain by Rudall Complex. Geological Province: Officer Basin.||||||25-JUL-07
31872|Tarcunyah Group|23742|4|Described|p6|Mesoproterozoic|Mesoproterozoic|Age: c.800 Ma. Underlain by Throssell Group. Geological Province: Paterson Orogen.||||||25-JUL-07
31872|Tarcunyah Group|23745|4|Described|p17|Neoproterozoic|Mesoproterozoic|Age: c.800 Ma. See also page 7 Fig 5. Of Yeneena Supergroup. Geological Province: Yeneena Basin.||||||
31872|Tarcunyah Group|23746|4|Described|p25|Neoproterozoic|Mesoproterozoic|||||||
31872|Tarcunyah Group|23757|5|Briefly described|p15|Neoproterozoic|Neoproterozoic|Includes the Eel Creek Formation. Age: <800Ma. Geological Province: Officer Basin.||||||07-JAN-08
31872|Tarcunyah Group|23758|5|Briefly described|p2 Fig 1|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
31872|Tarcunyah Group|23760|4|Described|p25|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
31872|Tarcunyah Group|23900|4|Described|p1538|Proterozoic|Proterozoic|Overlies both the Rudall Complex and the Throssell Group. Geological Province: Paterson orogen.||||||25-JUL-07
31872|Tarcunyah Group|24025|4|Described|p15|Neoproterozoic|Neoproterozoic|Age: c.800Ma.  Geological Province: Officer Basin.||||||
31872|Tarcunyah Group|24110|5|Briefly described|Plate 1|Proterozoic|Proterozoic|Geological Province: Officer Basin.||||||12-NOV-08
31872|Tarcunyah Group|24161|5|Briefly described|p6|||Unconformably overlies the Rudall Complex.||||||
31872|Tarcunyah Group|24194|5|Briefly described|p898, p899 Fig.2|Neoproterozoic|Neoproterozoic|Geological Province: Yeneena Basin||||||
31872|Tarcunyah Group|24197|5|Briefly described|p100|||Formerly of the Yeneena Group. Geological province: Paterson Orogen.||||||07-FEB-11
31872|Tarcunyah Group|24390|5|Briefly described|p12 Table 3|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
31872|Tarcunyah Group|24594|5|Briefly described|p602|Neoproterozoic|Neoproterozoic|Dominated by sandstone and conglomerate units with minor shale and carbonate beds.  Geological Province: Officer Basin (Paterson Orogen).||||||
31872|Tarcunyah Group|43848|5|Briefly described|Map Legend||Proterozoic|||||||
31872|Tarcunyah Group|43849|5|Briefly described|Map Legend||Proterozoic|||||||
31872|Tarcunyah Group|44111|6|Mentioned|p.55, p56 Fig.1, 57, p59, 60-61|||Does not display the metamorphism and deformation associated with the Miles Orogeny that is present in the underlying Throssell Group. Deformed by Paterson Orogeny. Faulted against or unconformably overlies Throssell Group. Partly coeval with Savory Group. Unconformably overlain by younger units of Savory Group. Includes Karara Formation. Late Proterozoic: between c.1200 and c.800 Ma. Contains Supersequence 1 stromatolites. Very sparsely mineralised, but has potential for hydrocarbons.||||||
31872|Tarcunyah Group|44189|5|Briefly described|Map legend||Proterozoic|||||||
31872|Tarcunyah Group|44190|5|Briefly described|Map Legend||Proterozoic|||||||
31872|Tarcunyah Group|44229|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Includes the Eel Creek Formation.  Age: c.800Ma.  Geological Province: Eel Creek Basin.||||||10-NOV-04
31872|Tarcunyah Group|44866|5|Briefly described|Map Legend||Neoproterozoic|||||||
31872|Tarcunyah Group|49895|4|Described|p9|Neoproterozoic|Neoproterozoic|Geological Province: Paterson Orogen, Officer Basin. Unconformably overlies the Throssell Group. See also p2 Fig.1.||||||24-JAN-06
31872|Tarcunyah Group|49911|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic| Age: c.800Ma.  Geological Province: Officer Basin.||||||
31872|Tarcunyah Group|50008|4|Described|p43|Neoproterozoic|Neoproterozoic|Age: c. 900Ma. Metasediments. Unconformably overlies Bangemall Supergroup and southeastern part of Yilgarn Craton. Formerly included in "Yeneena Group". Geol. Prov: Officer Basin. Source of sediment is probably Gascoyne Complex, based on detrital zircons.||||||12-JUN-07
31872|Tarcunyah Group|50085|5|Briefly described|p12 Tb. 3|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
31872|Tarcunyah Group|50188|5|Briefly described|p10 Fig. 3|Neoproterozoic|Neoproterozoic|Age: ~800Ma.||||||
31872|Tarcunyah Group|50228|5|Briefly described|p477|Neoproterozoic|Neoproterozoic|Unconformably overlies the Bangemall Supergroup. Part of the 840-700Ma Supersequence 1 of the Centralian Superbasin. Geological Province: Officer Basin.||||||
31872|Tarcunyah Group|50436|6|Mentioned|p1.1|||Of the Yeneena Group.||||||
31872|Tarcunyah Group|50544|4|Described|p57, p10 Fig. 5|Neoproterozoic|Neoproterozoic|Represented on YARRIE by Googhenama and Waroogunyah Fms.  Age: <800Ma.  Unconformably overlies Gregory Granitic Complex, and the Gorge Creek and Fortescue Gps.  Correlated with the Supersequence 1 of the Centralian Superbasin.  Geol: Prov:Officer Basin.||||||
31872|Tarcunyah Group|50555|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Includes the Waroongunyah Formation.  Age: c.800Ma.  Geological Province: Officer Basin.||||||21-JUL-04
31872|Tarcunyah Group|60429|5|Briefly described|p7, p25|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||07-FEB-11
31872|Tarcunyah Group|60470|4|Described|p1, 2-5, p8|Neoproterozoic|Neoproterozoic|in NW Officer Basin. Previously included in Yeneena Basin. Forms basal part of Centralian Superbasin.Unconformably overlies Bangemall Supergroup and Pilbara Craton units. In faulted contact with Throssell Range Group.  The stromatolites in the group belong to the Acadiella australica stromatolite assemblage of Grey & Stevens (1997), which is c.825 to 802 Ma old; detrital zircons give a maximum age for the basal part of the group of 1070 Ma. Consists of conglomerate, sandstone, siltstone, carbonate and evaporite.||||||
31872|Tarcunyah Group|61023|5|Briefly described|p16 Tb. 3|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||11-APR-08
31872|Tarcunyah Group|61732|5|Briefly described|p85, p131|||Now includes units which were part of the Yeneena Group, from the northeastern Officer Basin area.  Geological Province: western Officer Basin.||||||16-JUL-13
31872|Tarcunyah Group|62453|3|Fully described|p5 Fig. 3, p52, 63|Cryogenian|Cryogenian|Geological Province: Officer Basin/Paterson Orogen. Correlated with Buldya Group and Sunbeam Group. Unconformably overlies Rudall Complex. Unconformably overlain by Tchukardine Formation. ||||||
31872|Tarcunyah Group|62986|5|Briefly described|p18|||Forms the base of the northwestern Officer Basin. Metasedimentary units that unconformably overlie southeastern Pilbara Craton and eastern part of Bangemall Supergroup. Contains the Gunanya Sandstone.||||||
31872|Tarcunyah Group|62987|5|Briefly described|p30-31|||Geological Province: Paterson Orogen. Correlates with Buldya and Sunbeam Groups but is structurally separated from them due to the Paterson Orogen at 550Ma.||||||
31872|Tarcunyah Group|63139|5|Briefly described|p50|||Includes the Waltha Woora Formation.||||||
31872|Tarcunyah Group|63236|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Includes Eel Creek Formation. Geological Province: Officer Basin.||||||17-SEP-07
31872|Tarcunyah Group|63417|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Includes Googhenama, Waroongunyah, Brownrigg, Yandanunyah and Waltha Woora Formations. Age: c. 820Ma. Geological Province: Officer Basin (Centralia Superbasin).||||||23-JUL-07
31872|Tarcunyah Group|64283|5|Briefly described|p54 Fig. 4|Neoproterozoic|Neoproterozoic|See also the informal  Lower Tarcunyah Group reference.||||||16-JUL-13
31872|Tarcunyah Group|64286|5|Briefly described|p75 Fig. 3, p76 Fig. 4|Mesoproterozoic|Mesoproterozoic|Age: >1000Ma. Contains evaporites at top.||||||07-FEB-11
31872|Tarcunyah Group|64580|4|Described|map legend|Neoproterozoic|Neoproterozoic|Sandstone, siltstone, mudstone, and stromatolitic and non-stromatolitic dolomite; minor conglomerate; includes GOOGHENAMA, GUNANYA, KARARA, WATERS, WAROONGUNYAH, and CHOORUN FORMATIONS, BROWNRIGG SANDSTONE, YANDANUNYAH WONGARLONG, NOOLOO.||||||15-DEC-08
31872|Tarcunyah Group|64589|6|Mentioned|dated_samples file|||Officer Basin. Includes Choorun Formation.||||||
31872|Tarcunyah Group|64688|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Includes the Eel Creek Formation.  Geological province: Officer Basin.||||||
31872|Tarcunyah Group|64722|5|Briefly described|Fig. 2 p3-6, Fig 6 p15, p16|Neoproterozoic|Neoproterozoic|Yeneena Basin? Sedimentary unit located in the Paterson region. This article considers this unit part of the Centralian Superbasin system.||||||
31872|Tarcunyah Group|64724|5|Briefly described|p49 Fig. 7|Cryogenian|Cryogenian|Deposited in the Officer Basin during (and after) the Centralian 1 event (~840-824 Ma)||||||
31872|Tarcunyah Group|64725|6|Mentioned|p67.|Neoproterozoic|Neoproterozoic|Officer Basin||||||
31872|Tarcunyah Group|64772|5|Briefly described|Plate 1, p14 Fig. 7, p20-21 Fig.10|Neoproterozoic|Neoproterozoic|Age: c.800Ma. Undivided rocks - sandstone, siltstone, mudstone, and stromatolitic and non-stromatolitic dolomite; minor conglomerate. Shown adjacent to Spearhole Formation (Sunbeam Group) in Plate 1 [?lateral equivalent].||||||25-NOV-13
31872|Tarcunyah Group|64777|4|Described|p1-6|Neoproterozoic|Neoproterozoic|Formerly included in the obsolete Yeneena Group by Williams et al. (1976). Williams (1992) suggested a deformation constrained age of 1200-1000 Ma. Depositional age of 820 Ma based on correlations with the Adelaide Rift Complex (Bagas et al., 1995), and the occurrence of 800 Ma stromatolite assemblages (Grey and Steven 1997, Stevens and Grey 1997). SHRIMP U-Pb detrital zircon populations at 1780 Ma, 1310-1000 Ma, and a minor group from 1670 to 1310 Ma. Most likely sources are northern Gascoyne Complex and NW Paterson Orogen.|||Includes the Nooloo, Wongarlong, Yandanunyah, Waroongunyah and Googhenama Formations and the Brownrigg and Gunanya Sandstones.|Unconformably overlies the Bangemall Supergroup.|Conglomerate, sandstone, siltstone, carbonate and evaporites.|
31872|Tarcunyah Group|64793|6|Mentioned|p283, p291 fig 8, p293|||Of western Officer Basin. Previously regarded as part of the Paterson Orogen. Hosts Baicalia burra Stromatolite Assemblage at Constance Headland.|||Includes Waters Formation.|||
31872|Tarcunyah Group|64943|4|Described|p2-4,7,13-14,21,27-29,30,33,35-36,39|Neoproterozoic|Neoproterozoic|Includes Gunanya Sandstone and Choorun Formation. Deltaic to shallow-shelf sediments; c. 800 Ma (Bagas et al. 1995); unconformably overlies Rudall Complex. Max depositional age from underlying metamorphic biotite: 1194 Ma Rb/Sr (de Leter et al 1977).||||||
31872|Tarcunyah Group|65363|6|Mentioned|p9, p19.|||Northwestern Officer Basin. Correlated with Kanpa Formation on the basis of tentative identification of Baicalia burra in that unit.||||||
31872|Tarcunyah Group|65366|5|Briefly described|p24|||Northeastern Officer Basin. Includes the Acaciella australica Stromatolite Assemblage||||||
31872|Tarcunyah Group|65403|4|Described|p14, p13, p1, pp3-5, p19, p20, pp28-29.|Neoproterozoic|Neoproterozoic|Officer Basin. Duricrust formed on quartz arenite forms resistant plateau, cliff lines and narrow ravines and gorges. Shallow-water succession in a near-shore, ?marine environment. Age from stromatolites and acritarchs. Correlative of basal Savory Group.|c. 800 - 610 Ma.||Includes Karara, Waters, Choorun and Nooloo Formations and Gunanya Sandstone.|Unconformably overlies Rudall Complex, Gregory Granitic Complex, Manganese Subgroup, and Pungkuli Formation. Is faulted against Throssell Group. Is overlain unconformably by Savory Group.||29-SEP-15
31872|Tarcunyah Group|65404|6|Mentioned|p244, p245 Fig.1, p246 Fig.2|||||||||
31872|Tarcunyah Group|65410|6|Mentioned|p72.|||Thermal alteration of palynological samples indicates maturation to liquid petroleum to dry gas-generation phase.||||||
31872|Tarcunyah Group|65416|6|Mentioned|p137.|Late Proterozoic|Late Proterozoic|Officer Basin.||||||
31872|Tarcunyah Group|65454|4|Described|p1, p6-7, p9-12, p22, p30-31|Cryogenian|Cryogenian|Of Officer Basin. Most of this Group outcrops west of Vines Fault. Interpreted correlative of Supersequence 1 of Centralian Superbasin and Yeneena Basin sediments. Composed of Wongarlong, Yandanunyah, Brownrigg, Waroongunyah, Nooloo and Choorun Formations.|Age shown as 850 - 830 Ma, p7|||||21-APR-16
31872|Tarcunyah Group|65725|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Includes Googhenama Formation, Waroongunyah Formation, Brownrigg Sandstone and Yandanunyah Formation. Age <1070 Ma, probably from Waroongunyah Formation. Province: Officer Basin (Centralian Superbasin)||||||26-FEB-13
31872|Tarcunyah Group|65826|4|Described|p1, p5, pp10-11, p13. |Neoproterozoic|Neoproterozoic|Northwestern Officer Basin, Paterson Orogen. Correlated with Supersequence 1 of the Centralian Superbasin. A supratidal to shallow-water and locally fluviatile-deltaic sequence. Includes Acaciella australica stromatolites. The Miles Orogeny produced NW-trending folds and faults.|c.820 Ma (Bagas et al. 1995, 1999).||Includes Googhenama, Waroongunyah, Wongarlong, Nooloo and Yandanunyah Formations and Brownrigg Sandstone.|Unconformably overlies Bangemall Supergroup and Rudall Complex. Is faulted against the Throssell Range Group.||
31872|Tarcunyah Group|65829|6|Mentioned|p27.|||Re-mapping of PEARANA and BRAESIDE showed that the Waltha Woora Formation (of the Bangemall Group) was a westward extension of this unit (Williams and Trendall 1998a).||||||
31872|Tarcunyah Group|67183|4|Described|p640-41,643, 648-9,652, 656,665, 670-1|Neoproterozoic|Neoproterozoic|Officer Basin, Proterozoic, ~900 Ma. Flat-lying sediments. Age of ca 850 Ma is estimate of the basal part of the Group. Bagas et al. 1995, Grey et al. 2005. |base ca 850 Ma||Waltha Woora Formation, Googhenama Formation|Unconformably overlain by Paterson Formation, unconformably underlain by Balfour Formation.|Conglomerate, sandstone, siltstone, dolomite.|17-JUL-15
31872|Tarcunyah Group|67202|4|Described|p16, p54-55, p57, p64-66, p117, p124-125|Neoproterozoic|Neoproterozoic|See also p156-p157, p171, p229, p231-232, p234, p236-237, p243, p247, p272, p281. Officer Basin. Not strongly deformed except near major faults, and no significant metamorphism. Over 6km thick. Poorly magnetised and sediments not resolved in gravity data. Conductivity discussed and imaged. Appears as Tarcunyah Formation on p219.|||Googhenama, Waroongunyah, Yandanunyah, Wongarlong, Nooloo, Choorun, Waters, Karara, Pindinyah, Eel Creek Formations; Brownrigg, Gunanya Sandstones.|Unconformably overlies Gregory Range Suite, Fortescue Group and Throssell Range Group (and is faulted against the last). Faulted against the Jeerinah Formation.||15-FEB-18
31872|Tarcunyah Group|68902|5|Briefly described|p7, p12, p17|Neoproterozoic|Neoproterozoic|Crops out to the W of the Vines Fault. Deformed during the Paterson Orogeny.|Between ~860 Ma and ~810 Ma.|||||
31872|Tarcunyah Group|68981|6|Mentioned|p3 Fig.2|||Paterson Orogen.||||||
31872|Tarcunyah Group|69003|6|Mentioned|p4, p23, p60-61, p64|||Officer Basin, Paterson Orogen. Deformed by the c.650 Ma Miles Orogeny.||||||
31872|Tarcunyah Group|69167|6|Mentioned|geologyp_lut.csv|Neoproterozoic|Neoproterozoic||||Includes Waltha Woora Formation, Yandanunyah Formation, Brownrigg Sandstone, Waroongunyah Formation, Googhenama Formation|||
31872|Tarcunyah Group|69185|4|Described|GEOL_LUT_CSV files|Neoproterozoic|Neoproterozoic|Of Officer Basin. Also includes Nooloo Formation, Waters Formation, Waroongunyah Formation, Wongarlong Formation, Yandanunyah Formation. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|||Incldudes Brownrigg Sandstone, Chooruns Formation, Eel Creek Formation, Googhenama Formation, Gunanya Formation, Karara Formation.||Undivided; sandstone, siltstone, mudstone, and stromatolitic and non-stromatolitic dolomite; minor conglomerate.|
31872|Tarcunyah Group|69538|6|Mentioned|p533|Proterozoic|Proterozoic||||Includes Eel Creek Formation.|||
31872|Tarcunyah Group|69590|5|Briefly described|GEOL_LUT_CSV files|||Of Officer Basin (Phase 1), Centralian Superbasin. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|||Includes Brownrigg Sandstone, Eel Creek Formation, Googhenama Formation, Waltha Woora Formation, Waroongunyah Formation, Yandanunyah Formation.|||
31872|Tarcunyah Group|70936|6|Mentioned|p60-61|Cryogenian|Cryogenian|Geological province: Pilbara Craton. Previously thought to be correlable to Eel Creek Formation (Williams 1999, 2000), but invalidated by geochronological work by Wingate et al., 2012 and Rasmussen et al., 2012.||||||
31872|Tarcunyah Group|71003|6|Mentioned|p60-p61|Cryogenian|Cryogenian|Pilbara Craton. Previously correlated with the Eel Creek Formation, recent SHRIMP work shows a minimum age for that formation to be c 1070 M and invalidates any connection.||||||
31872|Tarcunyah Group|71042|5|Briefly described|p67-p69, p71|Neoproterozoic|Neoproterozoic|Officer Basin. Previously included the Waltha Woora Formation, the author has reassigned that unit to the Manganese Group on the basis of lithology and structural elements.|ca 830 - 850 Ma||Includes the Googhenama Formation.|||
31872|Tarcunyah Group|71169|6|Mentioned|p3 fig 2, p8, p11|Neoproterozoic|Neoproterozoic|Officer Basin.||||||
31872|Tarcunyah Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, conglomerate, siltstone, crystalline dolostone/dolomite|
31872|Tarcunyah Group|71795|6|Mentioned|p34 fig 3|||Paterson Orogen.||||||
31872|Tarcunyah Group|71894|6|Mentioned|p15|Neoproterozoic|Neoproterozoic|Pilbara Craton.||||||
31872|Tarcunyah Group|72034|5|Briefly described|500k_interpgeop16_lut|Cryogenian|Tonian|Gibson Sub-basin, Officer Basin (Phase 1).|||Includes Nooloo Formation, Wongarlong Formation, Yandanunyah Formation, Brownrigg Sandstone, Waroongunyah Formation, Waltha Woora Formation, Googhenama Formation, Choorun Formation, Karara Formation.||Sandstone, siltstone, mudstone, and stromatolitic and non-stromatolitic dolomite; minor conglomerate.|
68500|Tarlwa Pool Tonalite|63441|2|Defined|p9 Tb. 2|Archean|Archean|Of the Cleland Supersuite. Age: 3236+/-3Ma. Geological province: Pilbara Craton.||||||07-FEB-11
68500|Tarlwa Pool Tonalite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Cleland Supersuite.  Age: 3236Ma. Geological province: Karratha Terrane, West Pilbara Superterrane. Foliated hornblende-biotite tonalite; metamorphosed.||||||11-DEC-08
68500|Tarlwa Pool Tonalite|64580|4|Described|map legend||Paleoarchean|Of Cleland Supersuite. Foliated hornblende-biotite tonalite; metamorphosed.||||||15-DEC-08
68500|Tarlwa Pool Tonalite|67201|5|Briefly described|p14|||South of the Sholl Shear Zone.|3236 Ma|Cleland Supersuite||||25-NOV-16
68500|Tarlwa Pool Tonalite|69185|4|Described|500k_geologyp08_lut.csv||Paleoarchean|Geological Province: Pilbara Craton.||Unit of Cleland Supersuite.|||Foliated hornblende-biotite tonalite; metamorphosed|
68500|Tarlwa Pool Tonalite|70775|4|Described|p19, p24,  p25 tbl 4, p68|Paleoarchean|Paleoarchean|This unit outcrops in several inliers.|c. 3236 Ma|Cleland Supersuite||Unconformably overlain by the Fortescue Group.|Tonalite.|
68500|Tarlwa Pool Tonalite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||3236+/-3 Ma.|Cleland Supersuite|||Foliated hornblende--biotite metatonalite.|
39344|Tarmoola Granodiorite|24091|6|Mentioned|p52|||Geological Province: Yilgarn Craton.||||||
31155|Taurus Gabbro|43496|6|Mentioned|9|||||||||
68889|Taylor Lookout Granite|61056|5|Briefly described|p786|Mesoproterozoic|Mesoproterozoic|Age: 1788+/-6Ma.  Time equivalent of Twin Bonanza monzogranite.||||||
31773|Tching Granite|23569|4|Described|p6 Tb. 1|Archean|Archean|Of the Murchison Granite-Greenstone Terrane.   Amphibolite-facies monzogranite with inclusions of Bearra Gneiss||||||07-NOV-08
31773|Tching Granite|23574|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Cundarra Granite. Underlying unit Bearra Gneiss.||||||07-NOV-08
31773|Tching Granite|23576|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Cundarra Granite. Underlying unit Bearra Gneiss.||||||07-NOV-08
31773|Tching Granite|23577|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Cundarra Granite. Underlying unit Bearra Gneiss.||||||07-NOV-08
31773|Tching Granite|24114|5|Briefly described|p5 Fig.4|Archean|Archean|Geological Province: Yilgarn Craton. Age: c. 2680 Ma||||||07-NOV-08
31773|Tching Granite|43835|5|Briefly described|Map Legend|Archean|Archean|Age about 2680Ma.||||||07-NOV-08
31773|Tching Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
31773|Tching Granite|71269|6|Mentioned|1m_geologyp12_lut.csv||||||||Heterogeneous monzogranite with gneissic inclusions and 2965 Ma zircon xenocrysts; prograde amphibolite grade metamorphism.|
31773|Tching Granite|73526|6|Mentioned|p3|Neoarchean|Neoarchean|Collectively refers to a widespread exposure of granitic plutons in the NW Youanmi Terrane (previously Murchison Domain). See also Tching granite p4 Tb.1, age of 2680+/-3 Ma, 2689+/-4 Ma.|c. 2690 Ma|||||
24017|Tchintaby Dolomite Member|40088|6|Mentioned|p227|||||||||
24017|Tchintaby Dolomite Member|40089|2|Defined|p41|Mesoproterozoic|Mesoproterozoic|||||||
40435|Teague Granite|24578|5|Briefly described|p775|Paleoproterozoic|Archean|Age: ca 1300 Ma (Ar-Ar on K-feldspar) & ca 568 Ma (K-Ar on illite-smectite) & magmatic Crystallisation age of 2648 +/- 8 Ma (U-Pb, Nelson, 1997). Geological Province: Earaheedy Basin||||||07-NOV-08
40435|Teague Granite|50195|5|Briefly described|Map Legend|Paleoproterozoic|Archean|Age: c.2648Ma. Leucocratic K-feldspar granite. Geological Province: Yilgarn Craton.||||||15-DEC-08
40435|Teague Granite|61560|5|Briefly described|p491|Archean|Archean|Alkali-rich syenite composition.  Forms the core of the circular Shoemaker impact structure. Age: 2648+/-8Ma (Pirajno et al 2003). ||||||07-NOV-08
40435|Teague Granite|61564|5|Briefly described|p588, p590|Archean|Archean|Quartz-albite-orthoclase granite, locally mylonitised, with greenstone xenoliths. Age: 2648+/-8Ma (Nelson 1999). Geological Province: Yilgarn Craton.  See also p591 Fig. 3.||||||07-NOV-08
40435|Teague Granite|64580|4|Described|map legend|Proterozoic|Archean|Leucocratic K-feldspar granite and quartz syenite; within Shoemaker Impact Structure.||||||15-DEC-08
40435|Teague Granite|64772|4|Described|p7, p8 Fig. 4, Plate 1, p18 Fig. 8|Archean|Archean|Age: c.2648Ma. Geological province: Yilgarn Craton. Within Shoemaker Impact Structure. Origin discussed; more lithology included. See also p49.|||||Leucogranite and quartz syenite (Bunting et al. 1980); aegirine-augite-bearing orthoclase-albite granite or syenite (with pegmatite veins); albite-quartz-microcline granite or quartz syenite; and leucocratic alkali-feldspar granite (Pirajno 2002).|25-NOV-13
40435|Teague Granite|66427|5|Briefly described|p70-71 |Archean|Archean|Contains planar deformation features in quartz crystals; evidence for Shoemaker impact structure. Rb-Sr isochron ages of 1630 and 1260 Ma (Bunting et al., 1980).|2648 +/- 8 Ma (Nelson, 1999).||||Syenitic. Locally exhibits partial to pervasive silicification, fractures and metasomatic minerals.|
40435|Teague Granite|69152|5|Briefly described|500k_geologyp08_lut|Proterozoic|Archean||||||Leucocratic K-feldspar granite and quartz syenite; within Shoemaker Impact Structure.|07-AUG-15
40435|Teague Granite|70153|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean||2648 +/- 8 Ma (isotopic).||||Alkali feldspar granite; leucocratic.|
40435|Teague Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
40435|Teague Granite|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Yilgarn Craton, West Australian Craton. Events: Mulka Tectonic Event (570 - 570 Ma); Edmundian Orogeny D3e/M3e (995 - 954 Ma); Edmundian Orogeny (1026 - 954 Ma); Edmundian Orogeny D1e/M1e (1026 - 995 Ma); Edmundian Orogeny D2e/M2e (1026 - 995 Ma); Mutherbukin Tectonic Event (1321 - 1171 Ma); Mangaroon Orogeny (1682 - 1619 Ma); Mangaroon Orogeny D2m/M2m (1677 - 1659 Ma); Mangaroon Orogeny D1m/M1m (1682 - 1677 Ma); Ashburton Fold Belt D3a (1784 - 1772 Ma); Capricorn Orogeny D3n/M3n (1786 - 1772 Ma); Capricorn Orogeny (1817 - 1772 Ma); Ashburton Fold Belt D2a/M2a (1786 - 1784 Ma); Ashburton Fold Belt D1a/M1a (1794 - 1784 Ma); Capricorn Orogeny D2n/M2n (1808 - 1786 Ma); Capricorn Orogeny D1n/M1n (1813 - 1800 Ma); Glenburgh Orogeny D2 (1966 - 1947 Ma); Glenburgh Orogeny (2002 - 1947 Ma); Glenburgh Orogeny D1 (2002 - 1987 Ma); Ophthalmian Orogeny (2215 - 2145 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv.|1648+\-8 Ma||||Alkali feldspar granite; leucocratic|
40435|Teague Granite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Capricorn Orogen.|2648+/-8 Ma.||||Alkali feldspar granite; leucocratic.|
25521|Tean Formation|23383|4|Described|p21, p18 Tb. 2|Neoproterozoic|Neoproterozoic|Of Louisa Downs Gp. Fine- to medium-grained feldspathic sandstone and quartz wacke, interbedded with conglomerate and sst.  Conformably overlain by Lubbock Formation: conformably overlies McAlly Shale. Max. thickness: 120 m. Geol.Prov: Louisa Basin.||||||25-JAN-05
25521|Tean Formation|23599|4|Described|p18|Neoproterozoic|Neoproterozoic|Of Louisa Downs Group. Overlying unit Lubbock Formation. Underlying unit McAlly Shale. Geological Province: Louisa Basin. Max. thickness: 120 m.||||||
25521|Tean Formation|23601|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Louisa Downs Group. Overlying unit Lubbock Formation. Underlying unit: McAlly Shale. Geological Province: Louisa Basin. Max. thickness: 120 m.||||||25-JAN-05
25521|Tean Formation|23806|5|Briefly described|p1123 Fig. 2|Neoproterozoic|Neoproterozoic|Of Mount House Formation.||||||
25521|Tean Formation|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
25521|Tean Formation|32660|5|Briefly described|Table 6|||||||||
25521|Tean Formation|32728|6|Mentioned|Fig.16|||||||||
25521|Tean Formation|36551|6|Mentioned|Table 10|||||||||
25521|Tean Formation|36888|4|Described|p214|||||||||
25521|Tean Formation|36898|5|Briefly described|Table IV|||See also Fig.2B||||||
25521|Tean Formation|37927|6|Mentioned|Fig.2|||||||||
25521|Tean Formation|38157|6|Mentioned|Table X|||||||||
25521|Tean Formation|41429|6|Mentioned|p247|||||||||
25521|Tean Formation|44140|5|Briefly described|p301 fig 4-7, p303 Tb.4-2|Neoproterozoic|Neoproterozoic|Of Mount Ramsay area. 122 m thick. Probably equivalent to Nyuless Sandstone.||Louisa Downs Group||Conformably (?) overlies McAlly Shale. Is overlain conformably by Lubbock Formation.|Feldspathic sandstone, sub-greywacke; some conglomerate and dolomite.|08-MAR-18
25521|Tean Formation|44231|5|Briefly described|Map Legend|Neoproterozoic III|Neoproterozoic III|Of the Louisa Downs Group. Feldspathic sandstone, quartz wacke, quartz sandstone, pebble conglomerate, siltstone and shale; minor dolomite. Geological Province: Louisa Basin.||||||26-MAY-05
25521|Tean Formation|44397|14|Not recorded|p.15. Table 3||Adelaidean|Louisa Downs Group. Defn. on Tech.File E/52-9.||||||
25521|Tean Formation|44398|14|Not recorded|map legend||Adelaidean|||||||
25521|Tean Formation|44693|5|Briefly described|Map Legend||Proterozoic|||||||
25521|Tean Formation|44694|5|Briefly described|Map Legend||Proterozoic|||||||
25521|Tean Formation|45047|4|Described|p36|||Louisa Downs Group.||||||
25521|Tean Formation|48927|2|Defined|p30|Adelaidean|Adelaidean|||||||
25521|Tean Formation|63458|6|Mentioned|p873 Fig.2, p897 Fig.19. |Ediacaran|Ediacaran|||Unit in Louisa Downs Group.||||
25521|Tean Formation|67484|6|Mentioned|p294 Tb.1|Ediacaran|Ediacaran|Mount Ramsay area, West Kimberley. ||Of the Louisa Downs Group.||Overlain by Lubbock Formation. Underlain by McAlly Shale.||
25521|Tean Formation|67620|5|Briefly described|p5|Ediacaran|Ediacaran|Mount Ramsay area, Kimberley region.||Louisa Downs Group.||Overlies McAlly Shale. Is overlain by Lubbock Formation.||
25521|Tean Formation|68138|6|Mentioned|p156|Neoproterozoic|Neoproterozoic|Mount Ramsay area, Kimberley region.||Louisa Downs Group.||||
25521|Tean Formation|68244|4|Described|p660,665|Neoproterozoic|Neoproterozoic|Louisa Basin, Kimberley region.||Unit of Louisa Downs Group.||Overlain by Lubbock Formation. Underlain by McAlly Shale.|Conglomerate and sandstone.|
25521|Tean Formation|68473|6|Mentioned|p531|||Mount Ramsay. Part of the postglacial succession.||Louisa Downs Group||||
25521|Tean Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Cryogenian|Cryogenian|Louisa Basin||Louisa Downs Group|||Feldspathic sandstone, quartz wacke, quartz sandstone, pebble conglomerate, siltstone, and shale; minor dolomite.|04-AUG-15
25521|Tean Formation|69165|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran||||||Feldspathic sandstone, quartz wacke, quartz sandstone, pebble conglomerate, siltstone and shale. Minor dolomite.|
25521|Tean Formation|69634|4|Described|100k_interpgeop_lut.csv|Cryogenian|Cryogenian|Geological province: Halls Creek Orogen. Of Louisa Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1.|850-635 Ma (Biostrat)|Unit of Louisa Downs Group.|||Feldspathic sandstone, quartz wacke, quartz sandstone, pebble conglomerate, siltstone, and shale; minor dolomite|
25521|Tean Formation|70154|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran||541-635 Ma|Louisa Downs Group|||Feldspathic sandstone, quartz wacke, quartz sandstone, pebble conglomerate, siltstone and shale; minor dolomite.|
25521|Tean Formation|71267|4|Described|GEOL_LUT_CSV files|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Louisa Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|635-541 Ma (biostrat)|Unit of Louisa Downs Group.|||Mainly fine- to medium-grained feldspathic sandstone and quartz wacke, interbedded with conglomerate, fine- to medium-grained quartz sandstone, and laminated siltstone and mudstone; minor dolomite|
74838|Telegootherra Monzogranite|64891|5|Briefly described|p37 Fig. 2, p52-53 Tb. 1|Archean|Archean|Of Walganna Suite (Bald Rock Supersuite). Age: c. 2625Ma. Geological province: Murchison Domain. Monzogranite to syenogranite; post-tectonic.||||||07-FEB-11
74838|Telegootherra Monzogranite|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c.2623 Ma. |Unit in Walganna Suite.|||Monzogranite to syenogranite; undeformed, but with common igneous flow fabrics.|
74838|Telegootherra Monzogranite|67129|6|Mentioned|p19 fig 20|Archean|Archean|Murchison Domain, Youanmi Terrane.||Bald Rock Supersuite|||Monzogranite.|07-SEP-17
74838|Telegootherra Monzogranite|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. U-Pb zircon age: 2623+/- 9 Ma interpreted as the age of magmatic crystallization of the monzogranite. From geochron file 178197.1.pdf.||Walganna Suite|||Monzogranite to syenogranite; undeformed; common magmatic foliation. Monzogranite; medium- to coarse-grained; undeformed.|
74838|Telegootherra Monzogranite|69583|5|Briefly described|p49, p52; Plate 2|Neoarchean|Neoarchean|Murchison Domain.||Walganna Suite.|||Monzogranite to syenogranite.|
74838|Telegootherra Monzogranite|69584|5|Briefly described|p5 Fig.2|Neoarchean|Neoarchean|||Walganna Suite|||Monzogranite.|
74838|Telegootherra Monzogranite|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Walganna Suite.||||
74838|Telegootherra Monzogranite|69627|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton|c. 2623 Ma|Walganna Suite|||Monzogranite to syenogranite; undeformed; common magmatic foliation.|
74838|Telegootherra Monzogranite|70030|5|Briefly described|p191|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton.||Unit of Bald Rock Supersuite.||||
74838|Telegootherra Monzogranite|70796|4|Described|100k_geologyl_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 178197.1.pdf, Austin100_2442_stratig.pdf.|2623 +/ 9 Ma (isotopic)|Walganna Suite|||Monzogranite to syenogranite; undeformed; common magmatic foliation. Muscovitebearing monzogranite to syenogranite; medium to coarse grained; undeformed.|
74838|Telegootherra Monzogranite|70830|6|Mentioned|p8|||Murchison Domain. ||||||
74838|Telegootherra Monzogranite|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma). Sample GSWA 178197 (feldspar-phyric monzogranite) yielded a weighted mean 207Pb/206Pb date of 2620+\-6 Ma, interpreted as age of magmatic crystallization. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeol_lut.csv..|2623+\-9 Ma (isotopic)|Unit of Walganna Suite.|||Monzogranite to syenogranite; fine-grained and undeformed, muscovite-bearing pegmatitic, k-spar porphyritic, common magmatic foliation.|
74838|Telegootherra Monzogranite|71311|5|Briefly described|p798|||Northern Mount Magnet greenstone belt area.|2.62 Ga.|Bald Rock Supersuite.||||
74838|Telegootherra Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||2623+/-9 Ma.|Walganna Suite|||Monzogranite to syenogranite; undeformed; common magmatic foliation.|
40181|Telfer Granite|24594|5|Briefly described|p608 Fig. 4|Neoproterozoic|Neoproterozoic|Age: ~625Ma (U-Pb zircon, Nelson in Hickman and Clarke 1994).  Geological Province: Paterson Orogen.||||||10-SEP-12
36883|Telfer Member|23414|5|Briefly described|Map Legend|Neoproterozoic|Mesoproterozoic|Of Malu Formation, Yeneena Basin.||||||15-DEC-08
36883|Telfer Member|23758|4|Described|p8|Neoproterozoic|Neoproterozoic|Previously Telfer Formation. Of Malu Formation. Geological Province: Yeneena Basin. Max. thickness: 600 m.||||||
36883|Telfer Member|60470|4|Described|p9, 10-11|||Of Malu Formation. Distinguished by higher proportion of siltstone and rare carbonates near top. Transitional between Malu and overlying Puntapunta Formation.||||||
36883|Telfer Member|62453|5|Briefly described|p68|||Of the Malu Formation. Sandstone, siltstone, shale, carbonate. ||||||
36883|Telfer Member|64580|4|Described|map legend||Neoproterozoic|Of Malu Formation. Interbedded shale and dolomite; locally pyritic; minor carbonate rock.||||||15-DEC-08
36883|Telfer Member|65454|6|Mentioned|p30 Fig.A1b|Cryogenian|Cryogenian|Of Malu Formation||||||
36883|Telfer Member|65725|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Malu Formation. Interbedded sandstone and shale. Locally pyritic. Minor carbonate rock. Province: Yeneena Basin (Centralian Superbasin)||||||26-FEB-13
36883|Telfer Member|65826|4|Described|p13, p17.|||Represents a transition from deep water to an outer carbonate-shelf environment (represented by the overlying Puntapunta Formation). About 600 m thick. Hosts the Lamil Hills South and Egg gold prospects; mineralization is gossanous and fracture-controlled, with anomalous Au-Cu-Zn-As.||Unit at top of Malu Formation.||Transitional sequence below overlying Puntapunta Formation.|Fine- to medium-grained quartz sandstone interbedded with clayey sandstone, siltstone and shale; sandstone beds are well sorted, with minor authigenic dolomite; siltstone beds are laminated, commonly spotted with dolomite grains.|
36883|Telfer Member|67202|5|Briefly described|p191-193, p195,p198, p203,p208, p280-281|Neoproterozoic|Neoproterozoic|Bagas (2000). Hosts the Telfer Au-Cu deposit (described in detail). Domal structure and deformation described.||Malu Formation.||Is overlain transitionally by Puntapunta Formation.|Fine- to medium-grained sandstone interbedded with clayey sandstone, siltstone and shale, with minor dolomite near the top.|
36883|Telfer Member|69590|4|Described|500k_geologyp08_lut.csv|Neoproterozoic|Neoproterozoic|Geological province: Paterson Orogen. Events: Musgrave Orogeny; Paterson Orogeny. See 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.||Unit of Malu Formation.|||Interbedded shale and dolomite; locally pyritic; minor carbonate rock|
36883|Telfer Member|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone, shale, crystalline carbonate|
67988|Tern Formation|13222|6|Mentioned|p229.|Late Permian|Late Permian||||||Sandstone.|
67988|Tern Formation|13242|3|Fully described|p222-223,  p226 Fig. 8|Late Permian|Late Permian|Presented in 'defined' format. Supersedes Tern Mbr (Hyland Bay Fm). Of Hyland Bay Sub-group (Kinmore Gp). Contains 3 prograding sections, from basal shale to upper sandstone (detailed lithology incl.). Type section in Tern 1, 2521 - 2585 m.||||Unconformable on Dombey Fm; overlain probably unconformably by Penguin Fm.||21-DEC-12
67988|Tern Formation|60286|5|Briefly described|p273|Permian|Permian|Includes prograding shoreface succession. Contains Cruziana and Skolithos ichnofacies. Geological Province: Bonaparte Basin.||||||
67988|Tern Formation|64690|5|Briefly described|p504 Fig.2 |Late Permian|Late Permian|||Unit in Hyland Bay Sub-group.||Overlies Dombey Formation. Is overlain by Penguin Formation.||
67988|Tern Formation|64692|5|Briefly described|p521-535   |Late Permian|Late Permian|Bonaparte Basin. A wave-dominated, prograding shoreface succession deposited during highstand, truncated by a sequence boundary and overlain by a transgressive interval. Ichnology and sedimentology described in detail.||Unit in Hyland Bay Sub-group.||Overlies Dombey Formation. Is overlain by Penguin Formation.|Sandstones, mudstones.|
67988|Tern Formation|67370|5|Briefly described|pp313-317. |Late Permian|Late Permian|Bonaparte Basin. 3-D seismic images show dendritic channel-like features incised into the  top of this unit, suggesting near-horizontal depositional environment.||||Overlies Dombey Formation. Is overlain unconformably by Penguin Formation of the Mount Goodwin Subgroup.||
67988|Tern Formation|69452|3|Fully described|p36:8, 15, 20|Changhsingian|Wuchiapingian|Mory (1988); redefined in Gorter (1998). Petrel Sub-basin, Bonaparte Basin. 64m thick in the type section in offshore drillhole Tern-1. Offshore and prograding sandy shoreface to estuarine deposits. Up to 73m thick (offshore and onshore).||Hyland Bay Subgroup.||Unconformably overlies Dombey Formation. Is overlain unconformably by Penguin Formation.|Sandstone, siltstone and mudstone in repeating cycles.|12-JUL-16
67988|Tern Formation|69454|5|Briefly described|p38:4|Changhsingian|Wuchiapingian|Petrel Sub-basin, Bonaparte Basin.||Hyland Bay Subgroup.||||12-JUL-16
67988|Tern Formation|69653|6|Mentioned|p10|Changhsingian|Changhsingian|Petrel Sub-basin.||Hyland Bay Sub-group.||Overlies Dombey Formation. Is overlain by Penguin Formation.||
67988|Tern Formation|69673|6|Mentioned|p153 fig 125, p173|||||Hyland Bay Subgroup||Overlain by Penguin Formation, overlies Dombey Formation||
67988|Tern Formation|70061|5|Briefly described|Petrel Sub-basin Figs.2 & 3|Changhsingian|Changhsingian|See also Regional geology: Figs.6-8, p10. Vulcan: Fig.2. One of the most prospective hydrocarbon reservoirs within the central Petrel Sub-basin.||Hyland Bay Subgroup.||Overlies Dombey Formation. Is overlain by Penguin Formation.||12-JUL-16
67988|Tern Formation|70774|5|Briefly described|p5 fig 3|Changhsingian|Dzhulfian|Bonaparte Basin.||||||
67988|Tern Formation|71623|5|Briefly described|p355,359, p345 fig 2, p346, p352|Changhsingian|Changhsingian|Bonaparte Basin. Sonic logs shown in figures.||||Overlies truncated and eroded Hyland Bay Sub-group.|Sandstone.|
67988|Tern Formation|72505|5|Briefly described|p890|Changhsingian|Changhsingian|Southern Bonaparte Basin. Correlated to the Dulhuntyispora parvithola zone to P. Crenulata zone.||||Overlies the Dombey Formation. Overlain by the Penguin Formation.||12-MAR-20
67988|Tern Formation|73304|6|Mentioned|p77|||Bonaparte Basin.||||||
25524|Teronis Member|22754|5|Briefly described|p10 Tb. 2|Paleoproterozoic|Paleoproterozoic|Of the Elgee Siltstone.||||||07-NOV-08
25524|Teronis Member|23383|4|Described|p19, p18  Tb. 2|Paleoproterozoic|Paleoproterozoic|Of the Elgee Siltstone.  Interbedded dolomite. mudstone, siltstone, and quartz sandstone; some dolomite beds contain stromatolites.Max. thickness: 140m.  Geological Province: Kimberley Basin.||||||07-NOV-08
25524|Teronis Member|23601|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Elgee Siltstone (Kimberley Group).  Stromatolitic dolomite, sandy dolomite, oolitic dolomite, shale, micaceous siltstone, and fine-grained sandstone. Geological province: Kimberley Basin.||||||07-NOV-08
25524|Teronis Member|31662|5|Briefly described|p25|||||||||
25524|Teronis Member|32660|6|Mentioned|p230|||||||||
25524|Teronis Member|32728|5|Briefly described|p38|||See also Table 5||||||
25524|Teronis Member|34137|6|Mentioned|p10|||||||||
25524|Teronis Member|34462|4|Described|Table 1|||Carpentarian||||||
25524|Teronis Member|34463|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25524|Teronis Member|36551|6|Mentioned|p27|||||||||
25524|Teronis Member|36885|4|Described|p185|||||||||
25524|Teronis Member|37462|6|Mentioned|Fig.4.9|||||||||
25524|Teronis Member|38988|6|Mentioned|p16|||||||||
25524|Teronis Member|44140|5|Briefly described|p295, p298|Paleoproterozoic|Paleoproterozoic|0-140 m thick.||Locally at base of Elgee Siltstone.|||Dolomite, red shale, fine sandstone; abundant stromatolites.|08-MAR-18
25524|Teronis Member|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Elgee Siltstone (Kimberley Group). Stromatolitic dolomite, sandy dolomite, oolitic dolomite, shale, micaceous siltstone, and fine-grained sandstone. Age: >1790Ma. Geological Province: Kimberely Basin.||||||07-NOV-08
25524|Teronis Member|44363|4|Described|p.6,10,13|||(Carpentarian) mb Elgee Siltstone.||||||
25524|Teronis Member|44364|14|Not recorded|map legend|||||||||
25524|Teronis Member|44366|14|Not recorded|p.16, Table 2||Carpentarian|Part of Kimberley Group.||||||
25524|Teronis Member|44367|14|Not recorded|map legend|||(Reprinted 1971), part of Kimberley Group.||||||
25524|Teronis Member|44397|14|Not recorded|p.17, Table 2||Carpentarian|Kimberley Group.||||||
25524|Teronis Member|44398|14|Not recorded|map legend||Carpentarian|||||||
25524|Teronis Member|44694|5|Briefly described|Map Legend||Proterozoic|||||||
25524|Teronis Member|45047|5|Briefly described|p28|||Kimberley Group.||||||
25524|Teronis Member|64748|5|Briefly described|p269 Tb.1|Statherian||Locally at base of the Elgee Siltstone; 0-140m thick; Dolostone, mudstone, fine-grained sandstone; abundant stromatolites; ||||||
25524|Teronis Member|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Kimberley Basin||Elgee Siltstone|||Stromatolitic dolostone, sandy dolostone, oolitic dolostone, mudstone, micaceous siltstone, and fine-grained sandstone.|04-AUG-15
25524|Teronis Member|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Elgee Siltstone|||Stromatolitic dolostone, sandy dolostone, oolitic dolostone, mudstone, micaceous siltstone and fine grained sandstone.|
25524|Teronis Member|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Kimberley Basin. Events: King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1; King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1.|1835-1740 Ma (Inferred)|Unit of Elgee Siltstone.|||Stromatolitic dolostone, sandy dolostone, oolitic dolostone, mudstone, micaceous siltstone, and fine-grainedsandstone|
25524|Teronis Member|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1740-1835 Ma|Elgee Siltstone|||Stromatolitic dolostone, sandy dolostone, oolitic dolostone, mudstone, micaceous siltstone and fine grained sandstone.|
25524|Teronis Member|71267|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological provice: Halls Creek Orogen; King Leopold Orogen. Of Kimberley Basin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma).|1835-1740 Ma (inferred)|Unit of Elgee Siltstone.|||Stromatolitic dolostone, sandy dolostone, oolitic dolostone, mudstone, micaceous siltstone, and fine-grained sandstone|
25524|Teronis Member|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Elgee Siltstone.||Overlies Warton Sandstone.|Stromatolitic dolostone, sandy dolostone, oolitic dolostone, mudstone, micaceous siltstone, and fine-grained sandstone.|
74145|Tetlow Granite|66299|5|Briefly described|p14, p247, pp262-263.|Paleoproterozoic|Paleoproterozoic||1663 +/- 5 Ma. Regionally metamorphosed c.1280 Ma.|Unit in Durlacher Supersuite.||Forms thin layers and lenses within Davey Well Granite.|Strongly deformed aegirine-augite-  or hornblende- bearing metamorphosed quartz-diorite and metatonalite; scattered inclusions of amphibolite.|
74145|Tetlow Granite|67373|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.||Unit in Durlacher Supersuite.|||Aegirine-augite- or hornblende-bearing metamorphosed quartz diorite and metatonalite; scattered inclusions of amphibolite.|
74145|Tetlow Granite|68521|5|Briefly described|Map Legend|Statherian|Statherian|Geochronology from Sheppard et al. (2005).|c.1680-1620 Ma|Of the Durlacher Supersuite.|||Aegirine-augite- or hornblende-bearing quartz metadiorite and minor metatonalite; scattered inclusions of amphibolite.|
74145|Tetlow Granite|68522|5|Briefly described|Map Legend|Statherian|Statherian|Gascoyne Province. Geochronology from Sheppard et al.(2005).|1680-1620 Ma|Of the Durlacher Supersuite.|||Aegirine-augite- or hornblende-bearing metamorphosed quartz diorite and metatonalite; scattered inclusions of amphibolite.|
74145|Tetlow Granite|69166|4|Described|100k_interpgeol_lut.csv|Paleoproterozoic|Paleoproterozoic|Age derived from sample of leucocratic metadiorite (183207.1.pdf)|1663 Ma +/- 5 Ma (SHRIMP)|Durlacher Supersuite|||Aegirine--augite- or hornblende-bearing quartz metadiorite and minor metatonalite; scattered inclusions of amphibolite.|
74145|Tetlow Granite|70795|4|Described|100k_geologyl_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_interpgeol_lut.csv, 183207.1.pdf|1663 +/- 5 Ma||||Aegirine-augite or hornblende bearing quartz metadiorite and minor metatonalite; scattered inclusions of amphibolite. Leucocratic metadiorite, metaquartz diorite.|
74145|Tetlow Granite|70814|6|Mentioned|p68|||||||||
74145|Tetlow Granite|71869|5|Briefly described|p8, app p16|||Capricorn Orogen.|1662 +/- 5 Ma (igneous crystallisation age)|Durlacher Supersuite|||Metatonalite/quartz diorite.|
78758|Teutonic Bore Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2692 Ma (inferred).|Gindalbie Group|||Sedimentary rock; includes sandstone, siltstone, shale, and chert; metamorphosed. Felsic volcanic and volcaniclastic rock, basalt; metamorphosed.|
78758|Teutonic Bore Formation|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2692 Ma (inferred)|Unit of Gindalbie Group.|||Felsic volcanic and volcaniclastic rock; metamorphosed; Basalt; metamorphosed.|
30609|Texas Downs Formation|22440|6|Mentioned|p4|||||||||
30609|Texas Downs Formation|22547|4|Described|p22||Orosirian|Geological province: Texas Downs Basin. Includes beds formerly mapped as Red Rock beds or Mount Parker Sandstone. Dated 1800 Ma. 1000 m thick.||||||14-NOV-06
30609|Texas Downs Formation|22754|5|Briefly described|p10 Tb. 2, p5 Tb. 1|Paleoproterozoic|Paleoproterozoic|Overlies Red Rock Formation.||||||07-NOV-08
30609|Texas Downs Formation|24173|6|Mentioned|p22|||Unconformably overlies McHale Granodiorite. Of Tyler et al (1997b), assigned to Kimberley Group by Blake (1997).||||||06-APR-05
30609|Texas Downs Formation|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Sandstone, pebbly sandstone, conglomerate, siltstone, siltstone, mudstone, basalt and basaltic breccia. Geological Province: Texas Downs Basin.||||||15-DEC-08
30609|Texas Downs Formation|43853|5|Briefly described|Map Legend||Proterozoic|||||||
30609|Texas Downs Formation|43855|5|Briefly described|Map Legend||Proterozoic|||||||
30609|Texas Downs Formation|44230|5|Briefly described|Map Legend||Proterozoic|||||||
30609|Texas Downs Formation|44868|5|Briefly described|Map Legend||Proterozoic|||||||
30609|Texas Downs Formation|63866|5|Briefly described|p132|||||||Unconformably overlies the McHale Granodiorite. Possibly equivalent to the Kimberley Group.||
30609|Texas Downs Formation|64580|4|Described|map legend||Paleoproterozoic|Sandstone, pebbly sandstone, conglomerate, siltstone, mudstone, basalt, and basaltic breccia.||||||15-DEC-08
30609|Texas Downs Formation|68078|6|Mentioned|p23, p24|||Broadly similar to lower Kimberley Group, may be broadly coeval.|1827 +/- 3 Ma |||Unconformably overlies the McHale Granodiorite||
30609|Texas Downs Formation|69003|6|Mentioned|p5, p19|||Lamboo Province, Halls Creek Orogen.||||||
30609|Texas Downs Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Texas Downs Basin|||Includes 3 unnamed members.||Fine- to coarse-grained sandstone, pebbly sandstone, poorly sorted, pebble to boulder conglomerate, siltstone, and mudstone, intercalated with massive to amygdaloidal basalt flows and basaltic breccia.|04-AUG-15
30609|Texas Downs Formation|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv. |||||Fine to coarse grained sandstone, pebbly sandstone,pebble to boulder conglomerate, siltstone and mudstone, intercalated with basalt flows and basaltic breccia; minor dolerite.|
30609|Texas Downs Formation|69585|6|Mentioned|p4-5|Statherian|Statherian|Lamboo Province.||||Probable equivalent of the Kimberley Group.||
30609|Texas Downs Formation|69597|6|Mentioned|p5 fig 2b|||||||||
30609|Texas Downs Formation|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Texas Downs Basin. Events: King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|1827-1784 Ma (Inferred)||||Fine- to coarse-grained sandstone, pebbly sandstone, thin- to thick-bedded quartz sandstone, pebble to boulder conglomerate, siltstone, and mudstone, intercalated with massive to amygdaloidal basalt flows and basaltic breccia, and dolerite|
30609|Texas Downs Formation|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv.|1784-1827 Ma||||Fine to coarse grained sandstone, pebbly sandstone, conglomerate, siltstone and mudstone intercalated with basalt and basaltic breccia.|
30609|Texas Downs Formation|70731|6|Mentioned|p268|Stathetian|Stathetian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.||||||
30609|Texas Downs Formation|70812|5|Briefly described|p6|Statherian|Orosirian|Central and Eastern zones of the Halls Creek Orogen, Lamboo Province.|c. 1800-1750 Ma|||||
30609|Texas Downs Formation|70851|5|Briefly described|p4|Paleoproterozoic|Paleoproterozoic|Central and Eastern zones, Lamboo Province.|c. 1800-1750 Ma|||||
30609|Texas Downs Formation|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Texas Downs Basin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|1827-1784 Ma (inferred)||||Fine- to coarse-grained sandstone, thin- to thick-bedded quartz sandstone, pebbly sandstone, poorly-sorted conglomerate, siltstone, and mudstone, intercalated with massive to amygdaloidal basalt flows and basaltic breccia, and dolerite|
30609|Texas Downs Formation|71397|6|Mentioned|p5|Proterozoic|Proterozoic|Geological province: Central and Eastern zones, Lamboo Province, Halls Creek Orogen.||||||
30609|Texas Downs Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Texas Downs Basin.|||||Fine- to coarse-grained sandstone, pebbly sandstone, conglomerate, siltstone, and mudstone, intercalated with basalt flows and basaltic breccia.|
80135|The Bore Granite|69583|5|Briefly described|p154|||Youanmi Terrane. Post-tectonic, low-Ca granite; typically non-reflective and appears as thin sheets in seismic profiles.||||||
30172|Theatre Rocks Monzogranite|43102|5|Briefly described|Fig.5|||||||||
30172|Theatre Rocks Monzogranite|60076|5|Briefly described|p46 App. 1|||[Agmtr]   Subequigranular, fine- to medium-grained biotite monzogranite to granodiorite.||||||
30172|Theatre Rocks Monzogranite|65258|5|Briefly described|Map Legend|Archaean|Archaean|Subequigranular, fine- to medium-grained biotite monzogranite to granodiorite.||||||16-JUN-09
30172|Theatre Rocks Monzogranite|65264|5|Briefly described|p48 Appdx. 1|Archean|Archean|Fine- to medium-grained, equigranular biotite monzogranite to granodiorite.||||||07-FEB-11
30172|Theatre Rocks Monzogranite|65834|6|Mentioned|p5|||Norseman area.|c.2660 Ma (U-Pb zircon: Hill et al., 1992).|||||
30172|Theatre Rocks Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Fine- to medium-grained, equigranular biotite monzogranite to granodiorite; post-D2 to syn-D4.|07-AUG-15
30172|Theatre Rocks Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Fine- to medium-grained, equigranular biotite monzogranite to granodiorite; post-D2 to syn-D4.|
30172|Theatre Rocks Monzogranite|70802|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton.|||||Fine- to medium-grained, equigranular biotite monzogranite to granodiorite; post-D2 to syn-D4|
30172|Theatre Rocks Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, granodiorite|
30172|Theatre Rocks Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. See 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|||||Fine- to medium-grained, equigranular biotite monzogranite to granodiorite; post-D2 to syn-D4|
35232|Thelman Monzogranite|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Of the Pippingarra Granitoid Complex.  Geological Province: Pilbara Craton.||||||07-NOV-08
35232|Thelman Monzogranite|24110|5|Briefly described|Plate 1|Archean|Archean|Belongs to Pippingarra Granitoid Complex.  Geological Province: Pilbara Craton||||||07-NOV-08
35232|Thelman Monzogranite|24166|4|Described|p17|||Parent: Pippingarra Granitoid Complex||||||
35232|Thelman Monzogranite|24193|5|Briefly described|p875 Fig. 2|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
35232|Thelman Monzogranite|24327|5|Briefly described|Map Legend|Archean|Archean|Fine- to medium-grained muscovite (-garnet) monzogranite.  Parent: Pippingarra Granitoid Complex.   Age: c.2940Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
35232|Thelman Monzogranite|24349|5|Briefly described|Map legend|Archean|Archean|Of the Pippingarra Granitoid Complex.  Age: c.2940Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
35232|Thelman Monzogranite|63420|5|Briefly described|Map legend|Archean|Archean|Of Split Rock Supersuite. Geological Province: Pilbara Craton. Muscovite-biotite(-garnet) monzogranite; seriate to equigranular; fine- to medium-grained, massive to weakly foliated and metamorphosed.||||||07-NOV-08
35232|Thelman Monzogranite|63441|5|Briefly described|p11 Tb. 2|Archean|Archean|Of Sisters Supersuite. Geological province: Pilbara Craton.||||||07-FEB-11
35232|Thelman Monzogranite|68283|5|Briefly described|Map Legend|Archean|Archean|Pilbara Craton.||Of the Split Rock Supersuite.|||Muscovite-biotite(-garnet) monzogranite; equigranular to weakly porphyritic; fine to medium grained; massive to weakly foliated; metamorphosed.|23-SEP-13
35232|Thelman Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Muscovite--biotite(--garnet) monzogranite; equigranular to weakly porphyritic; fine  to medium grained; massive to weakly foliated; weakly metamorphosed.|
35232|Thelman Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; Split Rock Supersuite Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|2851-2831 Ma (inferred)|Unit of Split Rock Supersuite.|||Muscovite-biotite(-garnet) monzogranite; equigranular to weakly porphyritic; fine  to medium grained; massive to weakly foliated; weakly metamorphosed|
35232|Thelman Monzogranite|70775|5|Briefly described|p71, p81|||Mallina Basin. This unit occupies less than 10 km ^ 2. May be correlated with the Split Rock Supersuite, however it should be noted that geochronology is required to test this.|||||Massive to weakly foliated muscovite-biotite (and garnet) monzogranite. This unit is fine to medium grained, locally feldspar porphyritic and in many outcrops contains pegmatite dykes or sills.|
35232|Thelman Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
35232|Thelman Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Split Rock Supersuite|||Muscovite-biotite(-garnet) monzogranite; equigranular to weakly porphyritic; fine to medium grained; massive to weakly foliated; weakly metamorphosed.|
73634|Thirty Three Supersuite|66110|5|Briefly described|Map legend|Neoproterozoic|Mesoproterozoic|Age ranges from 995-954 Ma. Leucocratic medium-grained, muscovite-tourmaline(-biotite) monzogranite; equigranular to porphyritic.||||||
73634|Thirty Three Supersuite|66299|4|Described|p4 Fig.2, pp20-21, pp315-323.|Neoproterozoic|Mesoproterozoic|Northern part of Mutherbukin Zone in central Gascoyne Province. Low Zr content makes SHRIMP dating difficult and the source of the granites remains unknown. Zoned pegmatite dykes and sheets have been mined on a small scale for rare elements.|995 +/- 6 Ma to 954 +/- 12 Ma.|||Intrudes numerous units of Leake Spring and Pooranoo Metamorphics, and Durlacher and Moorarie Supersuites. Intruded by dykes of Mundine Well Dolerite Suite.|Porphyritic and leucocratic muscovite-biotite-tourmaline-bearing granite and metagranite, and pegmatites.|
73634|Thirty Three Supersuite|66887|5|Briefly described|p3 Fig.2, p5 Fig.4|Neoproterozoic|Mesoproterozoic|Southern Gascoyne Province.|~980-~910 Ma estimated from Fig.4.|||||
73634|Thirty Three Supersuite|66950|6|Mentioned|p9 Fig.8|Tonian|Tonian||c. 1000-900 Ma|||||
73634|Thirty Three Supersuite|67373|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||c.954 Ma.||||Muscovite-tourmaline pegmatite; local rare-element bearing pegmatite.|
73634|Thirty Three Supersuite|67843|6|Mentioned|p2 Fig.1. |Neoproterozoic|Mesoproterozoic|||||||
73634|Thirty Three Supersuite|68521|5|Briefly described|Map Legend|Tonian|Tonian|The two facies are mapped separately. Geochronology from Sheppard et al. (2007).|c.990-950 Ma||||Leucocratic, medium-grained, muscovite-tourmaline(-biotite) monzogranite, equigranular to porphyritic; muscovite-tourmaline pegmatite, some rare-element bearing.|
73634|Thirty Three Supersuite|68522|5|Briefly described|Map Legend|Tonian|Tonian|Gascoyne Province. 4 facies are mapped separately.|995-955 Ma||||Monzogranites; muscovite-tourmaline pegmatite; metamonzogranites.|
73634|Thirty Three Supersuite|69003|5|Briefly described|p4, p56|Neoproterozoic|Mesoproterozoic|Gascoyne Province, Capricorn Orogen. Associated with Edmundian Orogeny.|1030-925 Ma.||||Leucocratic metamonzogranite, tourmaline-bearing granite and pegmatite, REE-bearing pegmatites.|
73634|Thirty Three Supersuite|69011|5|Briefly described|Map Legend|Tonian|Tonian||995-955 Ma||||Includes muscovite-tourmaline pegmatite; some rare-element bearing.|
73634|Thirty Three Supersuite|69028|5|Briefly described|Map Legend|Tonian|Tonian||995-955 Ma||||Leucocratic granite and metagranite, and pegmatite.|06-MAY-14
73634|Thirty Three Supersuite|69080|5|Briefly described|p684, p690|Tonian|Stenian|Gascoyne Province. Associated with the Edmundian Orogeny.|1030-925 Ma.||||Leucocratic granite and metagranite, and RRE-bearing pegmatites.|
73634|Thirty Three Supersuite|69166|4|Described|geologyp_lut.csv|Neoproterozoic|Mesoproterozoic|Age derived from samples of pegmatites (190667.1.pdf)|939 +/-5 Ma  (SHRIMP) ||||Leucocratic medium-grained monzogranite. Medium grained, coarsely porphyritic biotite-tourmaline monzogranite, muscovite-tourmaline pegmatite. Foliated leucocratic muscovite metamonzogranite, foliated leucocratic biotite-muscovite metamonzogranite.|
73634|Thirty Three Supersuite|69387|4|Described|p3, p8, p12, p16-17, p22-24, p27-28|Tonian|Tonian|See also p37, p50, p68. Mutherbukin Zone, Gascoyne Province. Deformations (c.1320 Ma) discussed. SG and magnetic susceptibility values given. Gravity and magnetic modelling. Associated with high-grade W mineralisation at Nardoo Well.|995-940 Ma.|||Intrudes the Leake Spring and Pooranoo Metamorphics, and Durlacher Supersuite.|Strongly deformed, leucocratic granitic rocks and pegmatites. A-type (K-rich).|
73634|Thirty Three Supersuite|69596|5|Briefly described|p5, p9|Neoproterozoic|Neoproterozoic|Gascoyne Province. Associated with the 1030-955 Ma Edmundian Orogeny.|||||Leucocratic, tourmaline-bearing granites and pegmatites.|
73634|Thirty Three Supersuite|70795|4|Described|100k_geologyp_lut.csv|Neoproterozoic|Mesoproterozoic|Also 2_5m_interpgeop15_lut.csv, 100k_geologyl_lut.csv, 183287.1.pdf, 185945.1.pdf, 185946.1.pdf, West Australian Craton|1030-939 Ma|||Intrudes Morrissey Metamorphics, Pooranoo Metamorphics, Davey Well Granite|Leucocratic granite and metagranite, leucocratic medium grained muscovite-tourmaline monzogranite; equigranular to porphyritic pegmatite.|
73634|Thirty Three Supersuite|70826|6|Mentioned|p10|Neoproterozoic|Neoproterozoic|Capricorn Orogen.||||||
73634|Thirty Three Supersuite|71869|5|Briefly described|p3-p4|||Gascoyne Province. Emplaced during the Edmundian Orogeny.|1030-925 Ma||||Leucocratic, tourmaline-bearing granites and rare earth element-bearing pegmatites.|
73634|Thirty Three Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Neoproterozoic|Neoproterozoic||Max age ~995 Ma, min 939+/-5 Ma.||||Leucocratic granite and metagranite, and pegmatite.|
73634|Thirty Three Supersuite|72259|6|Mentioned|App. Tb.B||||||||Includes REE pegmatite and biotite-muscovite-tourmaline monzogranite.|
73634|Thirty Three Supersuite|73102|5|Briefly described|p3|||Gascoyne Province.|||||Leucocratic granite and metagranite, and pegmatite.|
73634|Thirty Three Supersuite|73214|5|Briefly described|p974 Fig.1|Neoproterozoic|Mesoproterozoic|Affected by the 920-830 Ma Reactivation Event and the c.570 Ma Mulka Tectonic Event.|1010-900 Ma.|||||
73634|Thirty Three Supersuite|73442|5|Briefly described|p3|||Gascoyne Province.|||||Leucocratic granite and metagranite, and pegmatite.|
24028|Three Corner Conglomerate Member|23047|6|Mentioned|35|||Of the Beasley River Quartzite. Hamersley Province.||||||10-FEB-09
24028|Three Corner Conglomerate Member|23280|6|Mentioned|Fig3p1086|||||||||
24028|Three Corner Conglomerate Member|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Beasley River Quartzite.||||||
24028|Three Corner Conglomerate Member|24544|5|Briefly described|p60|Paleoproterozoic|Paleoproterozoic|Base of Beasely River Quartzite. Geological Province: Hamersley Basin.||||||07-NOV-08
24028|Three Corner Conglomerate Member|35976|2|Defined|p110|Proterozoic|Proterozoic|Prob. Proterozoic||||||
24028|Three Corner Conglomerate Member|42260|6|Mentioned|p11|||||||||
24028|Three Corner Conglomerate Member|44152|6|Mentioned|p188 Fig.2-161, p189|||||Beasley River Quartzite||Overlies Kungarra Formation (unconformably).||
24028|Three Corner Conglomerate Member|66359|6|Mentioned|e96|||Of Beasley River Quartzite? Separated from the remainder of the formation by a sill at the eastern end of the Wyloo Dome.||||||
24028|Three Corner Conglomerate Member|66574|6|Mentioned|p920 Fig.9, p921, Fig.10|||Unit in Beasley River Quartzite (Wyloo Group).||||||
24028|Three Corner Conglomerate Member|68035|4|Described|p293, p292 fig 6|Paleoproterozoic|Paleoproterozoic|Ashburton Basin. Cut by dolerite dykes emplaced at 2.01 Ga.||Base of Beasley River Quartzite.||Unconformably overlies Kazput Formation, Turee Creek Group.|Contains abundant clasts of BIF, including pebbles of enriched ore derived from erosion of the Hamersley Group.|
24028|Three Corner Conglomerate Member|72712|5|Briefly described|p30-32, p34, p49.|Rhyacian|Rhyacian|Of Trendall (1979). Up to 100m thick in type section. Often incorrectly referred to as the 'Three Corners Conglomerate Member' (e.g. Van Kranendonk and Mazumder, 2013; Van Kranendonk et al., 2015b; Martindale et al., 2015) or the 'Three Corners Bore Conglomerate Member' (e.g. Krapez et al., 2017). Age range from parent Beasley River Quartzite.|< 2276 +/- 41 Ma to > 2208 +/- 10 Ma.|Beasley River Quartzite||Unconformably overlies Kungarra Formation.|BIF-pebble conglomerate. Includes BIF, hematite-enriched BIF clasts and chert pebbles derived mainly from the Weeli Wolli Formation, as well as lesser rhyolite and dolerite pebbles. Includes sandstones.|
24028|Three Corner Conglomerate Member|72758|6|Mentioned|p14 Table 1.|Paleoproterozoic|Paleoproterozoic|||Beasley River Quartzite|||Lithic conglomerate with minor sandstone and mudstone.|
34139|Three Mile Dolerite|22596|6|Mentioned|Table 1 p409|Archean|Archean|||||||07-NOV-08
34139|Three Mile Dolerite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2680 Ma (inferred).|Great Boulder Suite|||Differentiated gabbroic sill, leuco- to melanocratic, cumulate to granophyric, chilled margin; Quartz and hornblende rich granophyric gabbro, meso to leucocratic, ilmenite bearing; Coarse-grained melanocratic gabbro, stubby pyroxene-cumulate texture.|
34139|Three Mile Dolerite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2681 Ma (inferred)|Unit of Great Boulder Suite.|||Gabbro and leucogabbro; metamorphosed; leuco-melanocratic; stubby pyroxene cumulate texture, ilmenite-bearing, blue-coloured quartz phenocrysts.|
70719|Throssell Range Group|60470|4|Described|p1, 2-5, p8, 10-11, 12, 16|Neoproterozoic|Neoproterozoic|in Yeneena Basin, of Yeneena Supergroup, replaces Throssell Group. In faulted contact with Tarcunyah Group. A sandstone-shale-carbonate succession that unconformably overlies and locally faulted against Rudall Complex, formed in shallow water, fluviatile to marine-shelf environment. Max age 1070 Ma from detrital zircons.||||||
70719|Throssell Range Group|62453|5|Briefly described|p67|||Sandstone, shale, dolomite and limestone. Unconformably overlies: Rudall Complex. ||||||
70719|Throssell Range Group|62986|5|Briefly described|p18|Neoproterozoic|Neoproterozoic|Unconformable on the Palaeoproterozoic-Mesoproterozoic Rudall Complex. Geological Province: Yeneena Basin.||||||25-JUL-07
70719|Throssell Range Group|62987|6|Mentioned|p30|||In the Paterson Orogen.||||||
70719|Throssell Range Group|63417|5|Briefly described|Map legend|Neoproterozoic|Mesoproterozoic|Includes Broadhurst Formation and Coolbro Sandstone.  Geological Province: Yeneena Basin (Centralia Superbasin).||||||23-JUL-07
70719|Throssell Range Group|64722|5|Briefly described|Fig. 2 p3-6, Fig 6 p15, p16|Neoproterozoic|Neoproterozoic|Yeneena Basin. Sedimentary unit located in the Paterson region. This article considers this unit part of the Centralian Superbasin system. Shown as Throssell Group in Fig 6.||||||
70719|Throssell Range Group|64724|5|Briefly described|p49 Fig. 7|Cryogenian|Cryogenian|Deposited in the Yeneena Basin during (and possibly continuing after) the Centralian 1 event (~840-824 Ma)||||||
70719|Throssell Range Group|64725|5|Briefly described|p67.|Neoproterozoic|Neoproterozoic|Yeneena Basin. Separated from the Lamil Group by the Camel-Tabletop fault zone which extends southeast to the Musgrave Complex.|||Includes Broadhurst Formation and Coolbro Sandstone.|||
70719|Throssell Range Group|64777|4|Described|p1-6  |Neoproterozoic|Neoproterozoic|Formerly part of Yeneena Group. At least 750-720 Ma (Hickman and Bagas, 1998). SHRIMP U-Pb detrital zircon populations at 1780 Ma, 1310-1000 Ma, and a minor group from 1670 to 1310 Ma. Most likely sources are northern Gascoyne Complex and NW Paterson Orogen. Appears as Throssell Group in Fig.3.|750-720 Ma||Includes the Broadhurst Formation and the Coolbro Sandstone.|Unconformably overlies the Rudall Complex.|Sandstone-shale-carbonate succession.|
70719|Throssell Range Group|64941|5|Briefly described|p27|Tonian|Tonian|Yeneena Basin.|||Coolbro Sandstone|Overlain by Lamil Group units.|Coarsening up-sequence.|
70719|Throssell Range Group|65366|6|Mentioned|p22 Fig.2|Neoproterozoic |Neoproterozoic |||||||
70719|Throssell Range Group|65454|5|Briefly described|p7-8, p10-11|Cryogenian|Cryogenian|Of southwestern Yeneena Basin. Consists of Taliwanya, Pungkuli, Broadhurst and Isdell Formations, and Coolbro Sandstone.||||||
70719|Throssell Range Group|65725|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|In diagrammatic section, overlain by Paterson Formation. Contains Coolbro Sandstone and Broadhurst Formation. Age <1070 Ma , probably from Coolbro Sandstone, and older than Miles Orogeny (c.720 Ma). Province: Yeneena Basin (Centralian Superbasin)||||||26-FEB-13
70719|Throssell Range Group|65826|4|Described|p1, p5, p10, p12, p13, p17.|Neoproterozoic|Neoproterozoic|Yeneena Basin, Paterson Orogen. Formerly Yeneena Group and (informal) Throssell Group. Deformed by thrusts, recumbent folds and NW-trending folds and faults at 1132 +/- 21 Ma (Chin and de Laeter 1981); this event has subsequently been termed the Miles Orogeny (Bagas and Smithies 1998) and now thought to be c.720 Ma in age (Bagas et al. 2002). Correlative of Lamil Group. Hosts the Nifty Cu-Pb-Zn deposit and others.|c.820 - 654 Ma.||Includes basal Coolbro Sandstone and Isdell and Broadhurst Formations.|Unconformably overlies Rudall Complex. Is faulted against the Tarcunyah Group.||
70719|Throssell Range Group|67195|6|Mentioned|p6|||||||||
70719|Throssell Range Group|67202|4|Described|p5, p57-58, p60-64, p66, p121, p132,p141|Neoproterozoic|Neoproterozoic|See also p156, p176-177, p182-185, p194, p237-238, p243-244. Yeneena Basin. Appears as Throssel Range Group on p50 and p122, as Throssell Group on p5 and p141, and as Throssell Subgroup on p185 [?!]. Over 7km thick. Generalised lithological column on p58. Gravity and aeromagmetic interpretation. Conductivity image. Contains c.950 Ma detrital zircons.|c.860 Ma.|Yeneena Supergroup.|Coolbro Sandstone; Broadhurst, Isdell, Taliwanya, Pungkuli Formations.|Unconformably overlies the Rudall Complex. Is faulted against and overlain unconformably by the Tarcunyah Group. Is overlain by Lamil Group.||15-FEB-18
70719|Throssell Range Group|68902|5|Briefly described|p5 fig 3, p6, p7, p12, p17|Neoproterozoic|Neoproterozoic|Regionally metamorphosed, repeatedly deformed and intruded. c.4 km thick. Crops out to the E of the Vines Fault. Probably extends across the basement from W to E, possibly beneath the Lamil Group. Appears as Throssel Range Group in Fig. 4.||||Onlaps (overlies) or is in tectonic (fault) contact with Rudall Complex. Is unconformably overlain by the Paterson Formation.||
70719|Throssell Range Group|69003|4|Described|p4, p23, p61, p64, p66|||Yeneena Basin, Paterson Orogen. Underwent thrusting and recumbent folding during the c.650 Ma Miles Orogeny. Hosts the Nifty Cu deposit, currently the largest producer in WA (briefly described and compared with the Central African copper belt).|Betweeen c.980 Ma and c.845 Ma.||Coolbro Sandstone.||Includes chloritic and pyritic carbonaceous shales and siltstones.|
70719|Throssell Range Group|69167|4|Described|geologyp_lut.csv|Neoproterozoic|Mesoproterozoic||||Includes Broadhurst Formation, Coolbro Sandstone|||
70719|Throssell Range Group|69182|6|Mentioned|Ch4 p3|||Canning Basin. ||||||
70719|Throssell Range Group|69185|5|Briefly described|500k_geologyp08_lut.csv||||||Includes Broadhurst Formation.|||
70719|Throssell Range Group|69590|5|Briefly described|GEOL_LUT_CSV files + geochron files|||Geological province: Paterson Orogen. Of Yeneena Basin. Sample GSWA 172840 (coarse-grained sandstone) yielded an interpreted maximum depositional age of 2710+\-31 Ma for the sandstone (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 2_5m_geologyp98_lut.csv.|||Includes Broadhurst Formation, Coolbro Sandstone.|||
70719|Throssell Range Group|71080|6|Mentioned|p26|||Yeneena Basin. Probable Tonian age.|||Includes Coolbro Sandstone.|||
70719|Throssell Range Group|71169|6|Mentioned|p3 fig 2, p8|Neoproterozoic|Neoproterozoic|Yeneena Basin.||||||
70719|Throssell Range Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, shale, dolostone, limestone|
70719|Throssell Range Group|72034|5|Briefly described|500k_interpgeop16_lut|Cryogenian|Tonian|Yeneena Basin.|Max age 911+/-23 Ma.||||Sandstone, shale, limestone, and dolomite.|
78511|Throssell orthogneiss|68107|4|Described|p607 Fig.3, p617.|Neoarchean|Neoarchean|Yamarna Terrane. North of the Dorothy Hills Greenstone Belt. Not exposed; sampled from drill core. Contains xenocrysts dated at 2815-2800 Ma, 2775-70 Ma, and 2751 Ma (Cassidy 2007b).|2711 +/- 6 Ma (Cassidy 2007b).||||Granite gneiss.|
78988|Thundelarra Supersuite|70770|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c.2945 Ma.||Bunnawarra Suite.|||
78988|Thundelarra Supersuite|70796|5|Briefly described|2_5m_interpgeop15_lut.csv|Mesoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. Affected by the Yilgarn Craton granite magmatism (3010  2600 Ma); Youanmi Terrane events (3131  2600 Ma). See also 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 155879.1.pdf, 198213.1.pdf, 198240.1.pdf, 203702.1.pdf, 203703.1.pdf, Badja100_2240_stratig.pdf, Bungar100_2539_stratig.pdf.|||Includes the Bunnawarra Suite.|Unconformably overlain by the Wilgie Mia Formation.||
78988|Thundelarra Supersuite|70830|5|Briefly described|p9, p58|||Murchison Domain. Misspelt as the Thundalarra Supersuite on p58.|||Includes the Bunnawarra Suite.|||
78988|Thundelarra Supersuite|71269|4|Described|GEOL_LUT_CSV files + geochron files|||Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Oldest metamorphosed basement unit in the Murchison Domain, coeval with the oldest recognized felsic metavolcanic rocks, represented by the Madoonga, Gossan Hill, and Mount Gibson Formations (Van Kranendonk et al., 2013). Sample GSWA 198240 (polymictic metavolcanic breccia) yielded a weighted mean 207Pb/206Pb date of 2972+\-4 Ma, interpreted as the magmatic crystallization age of a dominant volcanic component of the breccia. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv.|||Includes Bunnawarra Suite, Gnows Nest Granodiorite.||Migmatitic tonalite to granodiorite gneisses with metagranitic leucosomes.|
78988|Thundelarra Supersuite|71272|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|||Gnows Nest Granodiorite.|||
73571|Tims Thicket Limestone|62020|5|Briefly described|p177-190|Pleistocene|Pleistocene|Yalgorup Plain, southern Perth Basin. Diverse fossil foraminifera assemblage (listed). Paleoecological interpretations discussed.|||||Weakly cemented limestone.|
73571|Tims Thicket Limestone|63454|2|Defined|p70, p71 Tb. 2|Pleistocene|Pleistocene|Includes White Hill Road and Clifton Downs Members. Unconformable over Myalup sand in east. Calcarenitic aeolianite; beach, marine and forameniferal calcarenites and shelly/bioturbated calcarenite with seagrass assemblage biota. On the Yalgorup Plain.||||||
73571|Tims Thicket Limestone|67135|6|Mentioned|p62, p63 Fig.85.|Pleistocene|Pleistocene|Occurs as a series of prominent ridges parallel to the coast.||||||
73571|Tims Thicket Limestone|73206|4|Described|p856-860, p862, p864-865|Pleistocene|Pleistocene|Of Semeniuk (1997). Yalgorup Plain; restricted to the southern part of the central Swan Coastal Plain. Distinct from Tamala Limestone. Overlain by Youdaland [landform]. Wedge-shaped to lensoid in plan view, where the seaward-edge forms a series of cusps. Shoaling upwards sequence records seagrass bank to beach to eolian facies (same as Kooallup Limestone). Includes a number of important smaller-scale features [see article]. Highly productive warm-water accumulation (supported by modern foram analogues) at a mean sea level ca. 3m above present mean sea level. [Article includes detailed discussion on geoheritage significance].||||Unconformably overlain[?] by Myalup Sand.|Limestone and intercalated sediments. Shoaling sequence including a lower, rich biofacies of shelly/fossiliferous limestone sharply overlain by beach facies containing swash zone molluscs, and an upper eolian unit.|
24525|Tindall Limestone|9324|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Daly River Group. Limestone, fine-grained, crystalline, dolomitic, algal and cherty in part with layers of quartz arenite and siltstone.||||||
24525|Tindall Limestone|14019|5|Briefly described|p20|Middle Cambrian|Middle Cambrian|Fossiliferous unit.  Overlies the Antrim Plateau Volcanics.||||||
24525|Tindall Limestone|22809|4|Described|20|||||||||
24525|Tindall Limestone|22810|4|Described|Table3 P7, P19|Ordovician|Cambrian|Maximum thickness 124.3m. Overlies Tolmer Group.||||||11-DEC-06
24525|Tindall Limestone|22813|5|Briefly described|Map|Cambrian|Cambrian|Part of the Daly River Group. Siltstone, limestone, mudstone, packstone, arkosic sandstone and conglomerate.||||||19-OCT-05
24525|Tindall Limestone|23216|4|Described|p3-4,Table1p7,37-42||Middle Cambrian|Of the Daly River Group. Age by Opik (1956).||||||19-JAN-06
24525|Tindall Limestone|23328|5|Briefly described|1030|Middle Cambrian|Early Cambrian|||||||07-SEP-09
24525|Tindall Limestone|23714|5|Briefly described|p7 Table 1.|Paleozoic|Paleozoic|See also page 36. Of Daly River Group. Max. thickness: 180 m.||||||07-NOV-08
24525|Tindall Limestone|23715|5|Briefly described|Map legend||Paleozoic|||||||07-NOV-08
24525|Tindall Limestone|24047|5|Briefly described|p62|Cambrian|Cambrian|Overlain by Petrel Formation.  Geological Province: Dunmarra Basin.||||||
24525|Tindall Limestone|24122|3|Fully described|p13, p3, Fig. 2|Cambrian|Cambrian|Of Daly River Group. Conformably overlain by Jinduckin Formation. Approximately 180m. thick.  Limestone, mudstone.  Geological Province: Daly Basin.||||||
24525|Tindall Limestone|24297|5|Briefly described|p19|Middle Cambrian|Middle Cambrian|Lateral equivalent of Montejinni Limestone. Geological Province: Daly Basin.||||||
24525|Tindall Limestone|24300|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Daly River Group.   Geological Province: Daly Basin.||||||11-DEC-06
24525|Tindall Limestone|24303|5|Briefly described|p38, p39|||Geological Province: Daly Basin. Max. Thickness: 182.8m. Equivalent to Gum Ridge Formation.||||||
24525|Tindall Limestone|28255|6|Mentioned|p94-95, p82|||Correlated with Headleys Limestone.  Geological Province: Day River and Wiso Basins.||||||15-JUN-05
24525|Tindall Limestone|29591|6|Mentioned|p107|||||||||
24525|Tindall Limestone|30003|6|Mentioned|p14|||Geological Province: Daly River Basin.||||||19-APR-05
24525|Tindall Limestone|31572|6|Mentioned|p22|||M.Camb.||||||
24525|Tindall Limestone|31917|6|Mentioned|Table 1|||M.Camb.||||||
24525|Tindall Limestone|32170|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
24525|Tindall Limestone|32171|6|Mentioned|p8|||Mid Cambrian||||||
24525|Tindall Limestone|32700|4|Described|Table 2|||||||||
24525|Tindall Limestone|32775|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Fossiliferous limestone and dolomitic limestone.||||||02-DEC-04
24525|Tindall Limestone|33373|3|Fully described|p10|||On Table 3.||||||
24525|Tindall Limestone|33374|6|Mentioned|p13|||Correlation||||||
24525|Tindall Limestone|33376|6|Mentioned|Map legend|Early Ordovician|Middle Cambrian|Middle Cambrian to Lower Ordovician||||||
24525|Tindall Limestone|34051|5|Briefly described|Table 1|||L.- M.Camb. See also pp6,8,12,13.||||||11-DEC-06
24525|Tindall Limestone|34052|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
24525|Tindall Limestone|34053|6|Mentioned|p8|||L.- M.Cambrian||||||
24525|Tindall Limestone|34438|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
24525|Tindall Limestone|34439|5|Briefly described|Table 1|||M.Camb. See also pp9,11.||||||11-DEC-06
24525|Tindall Limestone|34440|5|Briefly described|Table 1|||M.Camb. See also pp9,10.||||||11-DEC-06
24525|Tindall Limestone|34441|6|Mentioned|p12|||M.Camb. Correlate||||||
24525|Tindall Limestone|35224|6|Mentioned|p5|||||||||
24525|Tindall Limestone|35231|6|Mentioned|p8|||||||||
24525|Tindall Limestone|36335|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|Middle Cambrian(Ordian).||||||
24525|Tindall Limestone|38267|6|Mentioned|p84|||||||||
24525|Tindall Limestone|38902|6|Mentioned|p20|||||||||
24525|Tindall Limestone|39210|5|Briefly described|p48|||See also Fig.18||||||
24525|Tindall Limestone|39523|6|Mentioned|p95|||||||||
24525|Tindall Limestone|40136|6|Mentioned|p22|||See also p28.||||||11-DEC-06
24525|Tindall Limestone|40168|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician. Of the Daly River Group. Massive thinly bedded limestone with chert bands and nodules in places.||||||18-OCT-05
24525|Tindall Limestone|40852|6|Mentioned|p37|||||||||
24525|Tindall Limestone|40957|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
24525|Tindall Limestone|41586|6|Mentioned|Map legend|Middle Cambrian|Early Cambrian|||||||
24525|Tindall Limestone|41660|5|Briefly described|Map legend|Cambrian|Cambrian|Of Daly River Group. Grey and beige dolomitic limestone, algal and cherty in part.||||||07-OCT-05
24525|Tindall Limestone|41661|4|Described|p23|||||||||
24525|Tindall Limestone|42012|1|Redefined|p42|Middle Cambrian||See also p15. [Listed as DEF when entered, but is RDEF of Randal (1962) CEBMar95]||||||11-DEC-06
24525|Tindall Limestone|42014|5|Briefly described|Map legend|Cambrian||||||||
24525|Tindall Limestone|42070|4|Described|p3|||||||||
24525|Tindall Limestone|42206|6|Mentioned|p260|||||||||
24525|Tindall Limestone|42267|6|Mentioned|Fig.3 P312|||||||||
24525|Tindall Limestone|42639|6|Mentioned|p46|||In the Daly Basin.||||||11-DEC-06
24525|Tindall Limestone|43140|4|Described|p4|||Of the Daly River Group.||||||11-DEC-06
24525|Tindall Limestone|43149|5|Briefly described|Map Legend|Ordovician|Cambrian|Of the Daly River Group.||||||11-DEC-06
24525|Tindall Limestone|43187|5|Briefly described|p2|||||||||
24525|Tindall Limestone|43652|6|Mentioned|p386||Middle Cambrian|||||||
24525|Tindall Limestone|43832|4|Described|31, Table7 p26|Templetonian|Ordian|Age Middle Cambrian (late Ordian - early Templetonian)||||||
24525|Tindall Limestone|44113|5|Briefly described|p240|Middle Cambrian|Middle Cambrian|Of the Daly River Group. Geological Province: Daly River Basin. Maximum Thickness: 152m.||||||
24525|Tindall Limestone|44161|14|Not recorded|p.47||Middle Cambrian|||||||
24525|Tindall Limestone|44201|14|Not recorded|p.10||Cambrian|L.M.Cambrian.||||||
24525|Tindall Limestone|44332|14|Not recorded|p.10,opp.6,map|||(D53-14).||||||
24525|Tindall Limestone|44333|14|Not recorded|map legend|||Middle Cambrian?||||||
24525|Tindall Limestone|44459|14|Not recorded|p.9,14, opp.p.6, map|||(E53-2).||||||
24525|Tindall Limestone|44460|14|Not recorded|map legend||Middle Cambrian|Middle Cambrian.||||||
24525|Tindall Limestone|45022|3|Fully described|p.102, 103.|Ordovician|Cambrian|On many pages.||||||11-DEC-06
24525|Tindall Limestone|45058|6|Mentioned|p18|||See also p19. Unit of Daly River Group||||||11-DEC-06
24525|Tindall Limestone|45064|3|Fully described|Table 1|||See also p20.||||||11-DEC-06
24525|Tindall Limestone|45148|6|Mentioned|Fig.4|||Daly River Basin. See also p24.||||||11-DEC-06
24525|Tindall Limestone|45168|6|Mentioned|p6|||||||||
24525|Tindall Limestone|46675|5|Briefly described|Map legend|Paleozoic|Paleozoic|Of the Daly River Group.  Fossiliferous limestone with minor chert nodules and bands.||||||07-NOV-08
24525|Tindall Limestone|46676|14|Not recorded|p.6||Middle Cambrian|M.Cambrian; unit of Daly River Group.||||||
24525|Tindall Limestone|46679|14|Not recorded|map legend|||Map legend, of Katherine, 1 mile (D53-9).||||||
24525|Tindall Limestone|46792|6|Mentioned|p53|||Stratigraphy||||||
24525|Tindall Limestone|48942|6|Mentioned|p82|||Correlation||||||
24525|Tindall Limestone|60685|5|Briefly described|p19|Middle Cambrian|Middle Cambrian|Lateral correlative of Montejinni Limestone. Geological Province: Daly River Basin.||||||
24525|Tindall Limestone|60990|6|Mentioned|p85|Middle Cambrian|Middle Cambrian|Daly Basin. Faunal links with Antarctica.||||||
24525|Tindall Limestone|62376|5|Briefly described|p38|Cambrian|Cambrian|Geological Province: Beetaloo Sub-Basin.||||||09-FEB-10
24525|Tindall Limestone|62787|6|Mentioned|p82 Fig. 3|Cambrian|Neoproterozoic|Geological Province: Daly Basin (NT).||||||07-FEB-11
24525|Tindall Limestone|63569|6|Mentioned|p123|Cambrian|Cambrian|Daly Basin. Contains lingulate brachiopods that correlate with Redlichia guizhouensis Zone of China.||||||
24525|Tindall Limestone|64816|5|Briefly described|p3 Fig.2|Cambrian|Cambrian||||||Limestone with intervals of siltstone.|
24525|Tindall Limestone|64975|6|Mentioned|p162 Fig.6.|Cambrian|Cambrian|||||||
24525|Tindall Limestone|65236|5|Briefly described|p3 Fig. 3, p4 Fig. 4|Cambrian|Cambrian|Geological province: Beetaloo Sub-basin.||||||04-JUN-09
24525|Tindall Limestone|65337|5|Briefly described|p94.|Middle Cambrian|Middle Cambrian|Daly Basin. Carbonates.||||Unconformably overlies Kalkarindji Volcanic Group.||
24525|Tindall Limestone|65339|5|Briefly described|p5 Fig.4. |||||Unit in Daly River Group.|||Sandstone, limestone.|
24525|Tindall Limestone|65342|6|Mentioned|p8, p9.|||Daly Basin and Beetaloo Sub-basin, Dunmarra Basin. Max. thickness at least 200 m.||||Overlies Jamieson Sandstone. Is overlain by Jinduckin Formation.||14-FEB-17
24525|Tindall Limestone|65344|6|Mentioned|p8, 13|||Of the Daly Basin.||||||
24525|Tindall Limestone|65345|5|Briefly described|p4.|||Daly Basin. Equivalent to the Gum Ridge Formation of western Georgina Basin, and to the Montejinni Limestone/Hooker Creek Formation/Lothari Hill Sandstone sequence in the Wiso Basin.||Unit in Daly River Group.|||Bioclastic, mottled, oncoid and stromatolitic limestone; minor mudstone and basal conglomerate, arkosic sandstone and siltstone.|
24525|Tindall Limestone|67186|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Daly River Group.||Is overlain by Jinduckin Formation.|Limestone, fine-grained, crystalline, dolomitic, and chert with layers of quartz sandstone and siltstone.|23-NOV-11
24525|Tindall Limestone|67352|6|Mentioned|p19|Middle Cambrian|Middle Cambrian|Daly Basin. Contains a widespread (NT-SA-Antarctica) fossil fauna.||||||
24525|Tindall Limestone|69018|6|Mentioned|p450 Fig.1b|||||||||
24525|Tindall Limestone|69418|6|Mentioned|p3:29|||Daly Basin. A number of barite veins occur, eg Mathison Creek deposit.||||||12-JUL-16
24525|Tindall Limestone|69437|5|Briefly described|p22:10-11|Series 2|Series 2|Daly Basin, Centralian B Superbasin. Sequence 1. Shallow-marine to peritidal deposits. Is correlated with Negri Subgroup; Thorntonia, Top Springs Limestones; Tarrara, Gum Ridge, Chandler and Border Waterhole Formations; Walbiri, Giles Creek Dolostones.||||Overlies Jindare Formation and Antrim Plateau Volcanics. Is overlain by Jinduckin Formation.||12-JUL-16
24525|Tindall Limestone|69438|5|Briefly described|p23:29|Middle Cambrian|Middle Cambrian|Daly Basin. Correlation based on a distinct positive excursion in stable carbon and oxygen isotopes.||||Time-equivalent to Giles Creek Dolostone (Amadeus Basin).||12-JUL-16
24525|Tindall Limestone|69443|6|Mentioned|p28:21|||Daly Basin.||||Correlated with Gum Ridge Formation.||12-JUL-16
24525|Tindall Limestone|69445|5|Briefly described|p30:5, 17|Middle Cambrian|Middle Cambrian|Kruse et al. (1994). Daly Basin.||||Unconformably overlies Antrim Plateau Volcanics (Kalkarindji Suite).||12-JUL-16
24525|Tindall Limestone|69446|3|Fully described|p31:1-6, 9|Middle Cambrian|Middle Cambrian|Oldest unit in the Daly Basin; widespread outcrops around its margins. Exposures include rugged karst terrain and isolated residuals. Open shelf marine, minor peritidal deposits. Up to 204m thick; is 180.7m thick in the type section in drillhole NTGS 86/1. Probably continuous with Montejinni Limestone (Wiso Basin) under cover. Strong species-level similarity with correlative faunas of Linnekar Limestone and Panton Formation (Ord Basin), and Montejinni Limestone and Hooker Creek Formation (Wiso Basin). Broadly age-equivalent to Top Springs Limestone, Gum Ridge Formation, Thorntonia Limestone and Border Waterhole Formation (Georgina Basin). Offset by steep normal faults. Is quarried on Elsey Station for quicklime and ground limestone. Contains stratiform and surficial barite deposits, some vein fluorite and insignificant phosphate, and uneconomic base metal occurrences.||Daly River Group.||Unconformably overlies Antrim Plateau Volcanics, Jindare Formation or Roper Group. Is overlain by Jinduckin Formation conformably or locally disconformably.|Grey mottled, oncoid, ribbon and bioclast limestone; minor intercalated maroon-green siltstone or dark grey mudstone, microbial laminite and stromatolitic boundstone. Rich fauna of trilobites, bradoriids, brachiopods, hyoliths, molluscs and sponges.|12-JUL-16
24525|Tindall Limestone|69447|6|Mentioned|p32:2|||Daly Basin. Has strong species-level correlative faunas with Montejinni Limestone and Hooker Creek Formation (Wiso Basin).||||||12-JUL-16
24525|Tindall Limestone|69448|6|Mentioned|p33:3|||Daly Basin.||||Correlated with Negri Subgroup (Ord Basin).||12-JUL-16
24525|Tindall Limestone|69561|5|Briefly described|p31, p32 fig 1, p33 fig 2, p33, p42|Ordian|Ordian|Limestone reef fossils. Trilobites (Redlichia and Xystridura which are age diagnostic), archaeocopides, brachiopods, hyoliths, molluscs and sponges (metazoans).||||Overlies Jindare Formation, Antrim Plateau Volcanics, overlain by Jinduckin Formation|Fossiliferous limestone.|
24525|Tindall Limestone|69673|4|Described|p191|Cambrian|Cambrian |204m thick.||Daly River Group||Overlain by Jinduckin Formation|Fossiliferous oncoid, ribbon and bioclast limestone with minor intercalated siltstone or mudstone, microbial laminite and stromatolitic boundstone.|
24525|Tindall Limestone|70380|4|Described|p743-746, p759|Middle Cambrian|Middle Cambrian|Daly Basin. Up to 204m thick. Ordian age from diagnostic trilobites Redlichia and Xystridura. Correlated with Top Springs and Thorntonia Limestones, and Gum Ridge and Border Waterhole Formations, of the Georgina Basin; also with Lothari Hill Sandstone, Hooker Creek Formation and Montejinni Limestone of the Wiso Basin. Shallow-marine to peritidal sediments. The upper surface represents a (carbonate-to-siliciclastic) major sequence boundary.||Daly River Group.||Unconformably overlies Antrim Plateau Volcanics or Jindare Formation, or Roper Group in the SE. Is overlain conformably (possibly locally disconformably) by Jinduckin Formation.|Grey mottled, oncoid, ribbon and bioclast limestone, with minor intercalated maroon-green siltstone or dark grey mudstone, microbial laminite and stromatolitic boundstone; richly fossiliferous.|
24525|Tindall Limestone|70752|6|Mentioned|p141|Cambrian|Cambrian|Daly Basin. Brachiopod species discussed. Series 2, Stage 4 (Ordian) age.||||||
24525|Tindall Limestone|70850|5|Briefly described|Map legend.|Cambrian|Cambrian|Daly Basin.||Daly River Group.|||Limestone and dolomitic limestone.|
24525|Tindall Limestone|70866|5|Briefly described|Map legend.|Cambrian|Cambrian|Daly Basin.||Daly River Group.||Is overlain conformably by Jinduckin Formation.|Part-dolomitised limestone with silt laminations, interbedded calcilutite and marl; bioclastic limestone, mudstone and siltstone; minor stromatolitic boundstone and cryptalgal laminite; local bioclastic grainstone, arkosic sandstone and conglomerate.|
24525|Tindall Limestone|70968|6|Mentioned|p75|Cambrian|Cambrian|Fence diagram of wells in Beetaloo Sub-basin.||||||
24525|Tindall Limestone|72718|6|Mentioned|p10, p14|Cambrian|Cambrian|Strongly disrupts seismic signals.|||||Karstic, partially-dolomitised limestone.|
24525|Tindall Limestone|73083|6|Mentioned|p16, p29-30|Cambrian|Cambrian|Daly and Wiso Basins.||||||
77862|Tindals Diorite|65834|6|Mentioned|p50|||Coolgardie district. Misleadingly appears as Tindals Group, despite being located in a metabasalt zone.||||||
77862|Tindals Diorite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2698 +/- 6 Ma (isotopic).||||Mesocratic granodiorite to diorite sills; locally garnetiferous; metamorphosed.|
77862|Tindals Diorite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). Sample GSWA 204190 (quartz metadiorite) yielded a weighted mean 207Pb/206Pb age of 2698+\-5 Ma, interpreted as magmatic crystallization age of the quartz diorite dyke. See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2698+\-6 Ma|||Intrudes into Coolgardie Supergroup.|Mesocratic granodiorite to diorite sills; locally garnetiferous; metamorphosed|
78536|Tinganoo Bay beds|13194|6|Mentioned|p385 Tb. 4-16|||Of Money Shoals Basin. Coeval with Jurassic Frigate Shale, Bonaparte Basin.||||||27-NOV-13
27280|Tinkers Dolomite|24183|6|Mentioned|p12|||Correlated with the Cheyne Springs Formation||||||
27280|Tinkers Dolomite|37016|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
27280|Tinkers Dolomite|39427|2|Defined|p4|Precambrian|Precambrian|||||||
27280|Tinkers Dolomite|40088|6|Mentioned|p227|||||||||
27280|Tinkers Dolomite|40900|6|Mentioned|p32|||||||||
27280|Tinkers Dolomite|44142|5|Briefly described|p326 Tb.4-5|||1000 m thick.||Uaroo Group.||Correlated with Kiangi Creek Formation.|Dolomite, possible volcanic rocks.|
27280|Tinkers Dolomite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||crystalline dolostone/dolomite, volcanic rock|
36772|Tjauwata Group|24442|5|Briefly described|p28, p29|||Geological Province: Musgrave Block.||||||
36772|Tjauwata Group|24496|5|Briefly described|p15|Mesoproterozoic|Mesoproterozoic|Age: 1080-1050 Ma. Volcanics and sediments deposited in a regional zone of transtensile shear. Equivalent to the Bentley Supergroup. Geological Province: Musgrave Block.||||||
36772|Tjauwata Group|24497|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
36772|Tjauwata Group|50321|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes: Karukali Quartzite, Tjuninanta Formation, Mount Harris Basalt, Puntitjata Rhyolite, Bloods Range Formation.||||||09-JUN-04
36772|Tjauwata Group|60660|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Bimodal volcanics and sediments. Equivalent to the Bentley Supergroup.||||||22-FEB-05
36772|Tjauwata Group|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes: Bloods Range Formation, Puntitjara Rhyolite, Mount Harris Basalt, Tjuninanta Formation and Wankari Volcanics.  Geological Province: Musgrave Block.||||||
36772|Tjauwata Group|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes metasediments, rhyolite and basalt. Geological Province: Musgrave Block.||||||14-JAN-05
36772|Tjauwata Group|61154|4|Described|p16, p3, p5 Tb. 1.|Mesoproterozoic|Mesoproterozoic|Comprises basal Karukali Qtzite, deformed sediments and bimodal volcanics which include: mafic and felsic volcanics; felsic tuffs; interlayered mafic volcancis; felsic volcanics; volcaniclastic sediments and quartz. Age: 1090-1040Ma. Geol.Prov: Musgrave Bl.||||||05-AUG-14
36772|Tjauwata Group|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the Karukali Quartzite, Tjuninanta Formation and Mount Harris Basalt.||||||11-DEC-06
36772|Tjauwata Group|61524|5|Briefly described|p17 Fig.1|Mesoproterozoic|Mesoproterozoic|Part of rift sequence along with Wankari Volcanics and Bloods Range Beds. Geological Province: Musgrave Province.||||||02-JUN-06
36772|Tjauwata Group|61733|5|Briefly described|p46|||Emplaced during the Warakurna igneous event at c.1.08-1.05 Ga.|||||Bimodal volcanics and associated rift sediments.|
36772|Tjauwata Group|61864|6|Mentioned|p18 fig 4|||Part of a rift sequence.||||||
36772|Tjauwata Group|62989|5|Briefly described|p39, p40|Mesoproterozoic|Mesoproterozoic|Age: 1090-1040Ma. Includes Karukali Quartzite, Tjuninanta Formation, Mount Harris Basalt, Bloods Range Formation and Wankari Volcanics. Overlain by Dean Quartzite.  Geological Province: Amadeus Basin. Hosts small Cu prospects.||||||05-AUG-14
36772|Tjauwata Group|63562|6|Mentioned|p341|Stenian|Stenian|Of Amadeus Basin.|c.1090-c.1040 Ma (Close et al., 2005).||Includes Mount Harris Basalt, Bloods Range beds and Dixon Range beds.|Correlated with Tollu Group.|Relatively thin package of sedimentary and bimodal volcanic rocks.|
36772|Tjauwata Group|63866|4|Described|p202-p203, p205-p206, p208, p212|Stenian|Stenian|Mulga Park Domain, Musgrave Province.||Bentley Supergroup|Includes the Tjuninata Formation, Mount Harris Basalt and the Puntitjata Rhyolite.||Sediments and bi-modal volcanics.|
36772|Tjauwata Group|64580|6|Mentioned|map legend|||||||||
36772|Tjauwata Group|64722|6|Mentioned|p17|Stenian|Stenian|Equivalent of Tollu Group therefore Stenian age inferred.||||||
36772|Tjauwata Group|64745|5|Briefly described|p373 Fig. 3|||Geol. Prov: Mulga Park Domain, Musgrave Province. See also name variations: Supercrustal, Supercrustals and supracrustal.||||||
36772|Tjauwata Group|65135|5|Briefly described|p16, p17|Stenian||Sequence of supracrustal rocks with a similar lithological range to Kunmarnara and Tollu Groups. Straddles WA and NT border. Unconformably underlies basal sedimentary rocks of Amadeus Basin. Includes Puntitjata Rhyolite, dated at 1075 +/- 3 Ma.||||||
36772|Tjauwata Group|65233|5|Briefly described|p2|||Thick package of sediments and volcanics unconformably overlies basement Musgrave Province.  Geological province: Amadeus Basin.||||||07-FEB-11
36772|Tjauwata Group|65256|2|Defined|piii, p8, p14 Fig. 10, p37|Tonian|Mesoproterozoic|New Name. Lower section equivalent to Bloods Range beds. >1km thick. Middle section intruded by Rowley Granophyre and Walu Granite. Correlative of Tollu Group; intruded by Hull Granite Suite and Alcurra dolerite.|1075+/-2.5 Ma (Pb-Pb zircon).||Includes Karukali Quartzite, Tjuninanta Formation, Mount Harris Basalt, Puntitjata Rhyolite, Bloods Range Formation.|Unconformably overlies Pottoyu Granite Suite; disconformably underlies Kulail Sandstone and Dean Quartzite;|Voluminous mafic volcanics, minor felsic volcanics, polymictic conglomerate, red beds and quartzite (elaborated in text).|24-MAR-15
36772|Tjauwata Group|65338|6|Mentioned|p59.|||Southwestern Amadeus Basin. Rift succession. |1090 - 1040 Ma.|||||
36772|Tjauwata Group|65385|5|Briefly described|pS132|Stenian|Stenian|In western Musgrave Province. ~1090-1040 Ma.||||||08-MAR-12
36772|Tjauwata Group|65833|5|Briefly described|p16|Stenian||Unconformably overlain by Amadeus Basin sediments. Similar lithological range to Kunmarnara and Tollu Groups. Straddles WA and NT border. Includes Puntitjata Rhyolite and Wankari Volcanics.||||||
36772|Tjauwata Group|65906|5|Briefly described|p6, p19-20|Mesoproterozoic|Mesoproterozoic|A package of deformed sediments and bi-modal volcanics: basal quartzite and conglomerate, basalt overlain by rhyolites and epiclastic sediments. Considered a correlative of the Bentley Supergroup volcanics and associated sediments. Depositional age of Puntitjata Rhyolite member: 1075 +/- 3 Ma (Edgoose et al., 2004). Includes Mount Harris Basalt and Wankari Volcanics.||||||
36772|Tjauwata Group|67128|5|Briefly described|p3, p18, p30|||Western Bloods Range. Basement to Amadeus Basin.|||KaruKali Quartzite, Mount Harris Basalt, Puntitjata Rhyolite, Wankari Volcanics.|||
36772|Tjauwata Group|67375|5|Briefly described|p7 Fig.4, p16 Fig.10, p41, p217, p230.|Mesoproterozoic|Mesoproterozoic|Incorporated and replaces the Bloods Range Beds and the Mount Harris Volcanics. A sequence of supracrustal rocks straddling the WA/NT border; correlated with Tollu Group.|1085 - 1040 Ma (Edgoose et al. 2004).||Includes Puntitjata Rhyolite.||Sequence of volcanic, volcaniclastic and clastic rocks.|
36772|Tjauwata Group|67553|5|Briefly described|p8,17,43,59|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Supracrustal sequence with similar lithological range to the Kunmarnara anf Tollu groups.||||Equivalent to Bentley Supergroup.||
36772|Tjauwata Group|67565|5|Briefly described|p38.|Stenian|Stenian|A rift succession in the southwestern Amadeus Basin.|1090-1040 Ma.|||||
36772|Tjauwata Group|68994|5|Briefly described|p18|||Underlies the southwestern Amadeus Basin.|1090-1040 Ma (Close et al. 2004).|||||13-JAN-17
36772|Tjauwata Group|68995|5|Briefly described|p3 Fig.1, p4 Fig.2, p5, p22|Stenian|Stenian|Bloods Range area. |c. 1075 Ma|Bentley Supergroup|Karukali Quartzite, Mount Harris Basalt||Intrusive and extrusive mafic rocks.|
36772|Tjauwata Group|68996|6|Mentioned|p5, p36, p45, 47, p48, p69|Mesoproterozoic|Mesoproterozoic|Depositional age range indicated.|1090-1040 Ma|||||
36772|Tjauwata Group|69003|6|Mentioned|p37|Mesoproterozoic|Mesoproterozoic|W Musgrave Province.||||||
36772|Tjauwata Group|69091|4|Described|p52 Fig.4.1, p58, p69-70, see comments|||In area to north and east of Warakurna and continuing into Northern Territory (Bloods Range area). See also p84, p88, p105, p106 Fig.5.7a,b, p107 Fig.5.8a, p109 Fig.5.10, p131 Fig.6.1, p136, p137-139 Figs.6.4-6.6.|||Karukali Quartzite, Mount Harris Basalt.|Equivalent to Kunmarnara Group; overlies Pitjantjatjara Supersuite.|Supracrustal rocks, bimodal volcanics.|11-JUL-16
36772|Tjauwata Group|69153|6|Mentioned|500k_geologyp08_lut.csv||||||Bloods Range Formation, Mount Harris Basalt|||
36772|Tjauwata Group|69436|4|Described|p21:1-4, 11-14, 19, 21|Mesoproterozoic|Mesoproterozoic|Close et al. (2003). Crops out between the Petermann Ranges and Bloods Range, northern Musgrave Province. Extrusive equivalent of the Giles Complex. The felsic volcanic rocks form a highly fractionated suite from a common source. Is structurally interleaved with Dean Quartzite in the Wankari Detachment Zone of the Petermann Nappe Complex. Hosts a few occurrences of secondary Cu minerals but with insignificant mineralisation at depth. Is a potential target for red-bed Cu mineralisation. Quartz veins and soil samples show encouraging Au anomalies.|1090-1040 Ma.||Karukali Quartzite; Tjuninanta, Bloods Range Formations; Mount Harris Basalt; Puntitjata Rhyolite; Wankari Volcanics.|Is intruded by Hull Suite. Is broadly correlated with Bentley Supergroup.|A package of deformed quartz-rich and volcanigenic sedimentary rocks, epiclastic rocks, and bimodal volcanic rocks. A-type.|12-JUL-16
36772|Tjauwata Group|69437|5|Briefly described|p22:12|||Musgrave Province. Interpreted as a rift-related succession.|1090-1040 Ma.|||||12-JUL-16
36772|Tjauwata Group|69438|5|Briefly described|p23:2, 8-9|||A rift succession underlying the SW Amadeus Basin.|1080-1050 Ma (Close et al., 2004).||Bloods Range Formation.|||12-JUL-16
36772|Tjauwata Group|69606|5|Briefly described|p4 fig 2, p5|Mesoproterozoic|Mesoproterozoic|Amadeus Basin.|||Dixon Range beds, Wankari Volcanics.||Sandstone.|15-SEP-22
36772|Tjauwata Group|69655|5|Briefly described|p3|Stenian|Stenian||c. 1090-1040 Ma|||||
36772|Tjauwata Group|69729|6|Mentioned|p66 Fig.1, p70, p79|||Bentley Basin: Bloods Range area in NT.||||||
36772|Tjauwata Group|69937|5|Briefly described|vi, p7, p9, p16, p28, ;p34|||Musgrave Province. One of the sediment sources for the Amadeus Basin.|1085-1040 Ma.||||Sedimentary and volcanic rocks.|
36772|Tjauwata Group|70018|4|Described|p233,235-236,239-240|Mesoproterozoic|Mesoproterozoic|Amadeus Basin. Extension and deposition occurred after initial uplift of Musgrave Block. Prominent erosional and angular unconformity with the overlying Kulail Sandstone and Dean Quartzite suggest a major basin reorganisation.|||Includes Bloods Range Formation, Wankari Volcanics, Puntitjata Rhyolite, Mount Harris Basalt, Tjuninanta Formation and Karukali Quartzite.||Bimodal volcanic sand coarse-grained siliciclastic rocks including conglomerates.|
36772|Tjauwata Group|70083|6|Mentioned|p206|||Musgrave Inlier.|1085-1020? Ma.||||Volcanic, pyroclastic and sedimentary rocks.|
36772|Tjauwata Group|70634|6|Mentioned|500k_geolgyp08_lut.csv|Mesoproterozoic|Mesoproterozoic||||Includes Bloods Range Formation, Mount Harris Basalt|||
36772|Tjauwata Group|70793|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Events: Giles Event (1085-1040 Ma); Areyonga Movement; Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Alice Springs Orogeny (450-295 Ma). See 500k_interpgeop14_lut.csv, 2_5m_interpgeop15_lut.csv.|1085-1040 Ma (inferred)|Unit of Bentley Supergroup.|Includes Bloods Range Formation, Mount Harris Basalt.||Metamorphosed sandstone and siltstone, and felsic and mafic schist derived from volcanic rock|
36772|Tjauwata Group|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Bentley Basin. ||Bentley Supergroup||||
36772|Tjauwata Group|70831|5|Briefly described|p3|||Bentley Basin.||||||
36772|Tjauwata Group|70839|5|Briefly described|p326-332,345|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province. Of Bentley Basin. Exposed along NW margin of Musgrave region and in inliers in SW Amadeus Basin (Edgoose et al., 2004) and as part of 30-60km wide belt of ranges immediate south of southern limit of Supersequence 4 deposits (this study). Emplaced within Ngaanyatjarra Rift (Evins et al., 2010; Aitken et al., 2012).|||Includes Dixon Range beds and Bloods Range Formation.|Overlain unconformably by Dean Quartzite and Kulail Sandstone, locally by Dixon Range beds.||
36772|Tjauwata Group|71080|6|Mentioned|p30 fig 21|Mesoproterozoic|Mesoproterozoic|Underlies Amadeus Basin in WA.|||||Dominantly sandstone.|
36772|Tjauwata Group|71088|5|Briefly described|p4, p6-p8|||Amadeus Basin. Deposited within the structural Ngaanyatjara Rift.||Bentley Supergroup|Includes the Dixon Range beds.|Equivalent to the Kunmarnara Group.||
36772|Tjauwata Group|71170|5|Briefly described|p5|||||||||
36772|Tjauwata Group|71210|5|Briefly described|p4-p5, p8-p9, p21, p51, p79, p113|||Musgrave Province.|c. 1090 Ma (Edgoose et al., 2004)||Includes the Mount Harris Basalt, Puntitjata Rhyolite and Wankari Volcanics.|||
36772|Tjauwata Group|71211|6|Mentioned|p6 fig 1.3, p7 fig 1.4|||See also p24 fig 2.1, p84 fig 3.1, p136 fig 4.1 , p233. ||Bentley Supergroup|Includes the Smoke Hill Felsic Volcanic and the Wankari Volcanics.|||
36772|Tjauwata Group|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Late-stage component of the Bentley Supergroup. See 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeol_lut.csv.|1073+\-7 Ma; 1026+\-26 Ma|Unit of Bentley Supergroup.|Includes Bloods Range Formation, Dixon Range Formation, Karukali Quartzite, Mount Harris Basalt, Puntitjata Rhyolite, Tjuninanta Formation, Wankari Volcanics, Warrupura Formation.|Underlain by Pitjantjatjara Supersuite.|Siliciclastic sedimentary and volcanic rocks; locally metamorphosed|
36772|Tjauwata Group|71279|6|Mentioned|p353|||Musgrave Province. Source of c.1.3 to 0.8 Ga zircons in Pertatataka Formation.||||||
36772|Tjauwata Group|71321|6|Mentioned|p5|||Geological province: Musgrave Province.||||||
36772|Tjauwata Group|71344|6|Mentioned|p1093|Stenian|Stenian|Marks initiation of Amadeus Basin?|~1080 Ma||||Bimodal volcanics and sedimentary rocks.|
36772|Tjauwata Group|71810|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|c.1044 Ma - c.1039 Ma.|||Is overlain by Heavitree Formation.|Siliciclastic metasedimentary and volcanic rocks; locally metamorphosed (section only).|
36772|Tjauwata Group|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Bentley Supergroup|Includes Mount Harris Basalt, Bloods Range Formation.||Metamorphosed siliciclastic sedimentary and volcanic rocks.|
36772|Tjauwata Group|72094|5|Briefly described|p3 Fig 2, p7-8, 17, 18|Stenian|Mesoproterozoic|Bentley Basin. Variably deformed rhyolitic subvolcanic rocks. Magmatic crystallisation ages: 1041+/-6 Ma, 1039+/-7 Ma. Summary table of zircon geochronology on p8 Table 1.||Unit of Bentley Supergroup.|Includes Karulaki Quartzite and Mount Harris Basalt.|Strongly folded ridges of Dean Quartzite interleaved with Tjauwata Group rhyolite-dominant rocks. Equivalent to Kunmarnara Group.|Includes variably deformed rhyolitic sub-volcanic rocks.|
36772|Tjauwata Group|72375|5|Briefly described|p5|Stenian|Stenian|Of Amadeus Basin.|c. 1090-1040 Ma|||Overlain by Dean Quartzite.||
36772|Tjauwata Group|72443|6|Mentioned|p737|||Bentley Basin.||||||
36772|Tjauwata Group|73086|6|Mentioned|p7|Neoproterozoic|Neoproterozoic|Amadeus Basin, southwest. Preserves a Neoproterozoic succession that represents the initial basin-forming rifting event.||||||
36772|Tjauwata Group|73437|6|Mentioned|p151|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Bentley Supergroup||||
24036|Tjingkulatjatjarra Formation|23602|6|Mentioned|p9|||||||||
24036|Tjingkulatjatjarra Formation|42278|4|Described|p37|||See also Fig.3||||||
24036|Tjingkulatjatjarra Formation|43118|6|Mentioned|p9|||||||||
24036|Tjingkulatjatjarra Formation|43348|5|Briefly described|P5|||||||||
24036|Tjingkulatjatjarra Formation|43697|6|Mentioned|p25|||Younger part of the Rudall Complex.  Quartzite and schist. This formation is not disrupted by orthogneiss as is the upper part of the complex; interpreted as being younger than both the composite orthogneiss and the Yandagooge Formation.||||||08-AUG-05
24036|Tjingkulatjatjarra Formation|65404|6|Mentioned|p247|||A division of the Talbot terrane by Clarke (1991).||||||
77239|Tjuni Purlka suite|66256|5|Briefly described|p4 Fig.3, p8-11, p18, see comments|Stenian|Ectasian|In Tjuni Purlka Tectonic Zone, west Musgrave Province. Geochemistry provided. SHRIMP whole rock Nd isotopic crystallization age range. Also misspelt as Tjuni Pulka suite. See also p22-32, p34, p38-39, p41, p43-44, p54 App.1, p60-62 App.3, p71 App.4.||Pitjantjatjara Supersuite||Veins and sheets of Tjuni Purlka suite cut and engulf rocks of Wirku Metamorphics and Wankanki Supersuite.|Schlieric biotite-orthophyroxene leucogranites; locally voluminous veins, dykes and sheets.|11-JAN-17
77239|Tjuni Purlka suite|67375|5|Briefly described|p6, p19 Fig.11. |Mesoproterozoic|Mesoproterozoic|A-type. Yb-enriched. Geochemistry has within-plate as well as ocean-ridge indicators.|1210-1150 Ma.|Unit in Pitjantjatjara Supersuite.|||A compositionally unique suite of schlieric leucogranites.|
77239|Tjuni Purlka suite|67553|4|Described|p9,20,27-28,31,33,82|Stenian|Ectasian|Geological province: Musgrave Province, North Australian Craton. Early Musgravian granite. Compositionally unique suite of rocks restricted to Tjuni Purlka Tectonic Zone (NW-trending zone of multigenerational c. 1220, 1075, and 550 Ma shearing. Crystallisation age from GSWA 185339 and 183509. Intruded into Wankanki Supersuite.|1210-1150 Ma|Unit of Pitjantjatjara Supersuite.|||Schlieric leucogranites.|
77239|Tjuni Purlka suite|69003|5|Briefly described|p37|Mesoproterozoic|Mesoproterozoic|W Musgrave Province.||Pitjantjatjara Supersuite.||||
77239|Tjuni Purlka suite|69091|5|Briefly described|p56, p64 Fig.4.10|||Of Smithies et al. (2010). Tjuni Purlka Tectonic Zone||Pitjantjatjara Supersuite|||A compositionally unique suite of schlieric leucogranites.|
77239|Tjuni Purlka suite|69729|5|Briefly described|p74 Fig.7, p77-78|||Geochemistry plots.||Pitjantjatjara Supersuite.|||A-type granites.|
75926|Tobin Formation|66119|5|Briefly described|Map legend|Archean|Archean|Yamarna Terrane, Yilgarn Craton. Metamorphosed sedimentary rock; undivided.||||||
75926|Tobin Formation|66120|5|Briefly described|Map legend|Archean|Archean|Yamarna Terrane, Yilgarn Craton. Sedimentary and felsic volcanic rocks; local intrusive rocks.||||||
75926|Tobin Formation|66121|5|Briefly described|Map legend|Archean|Archean|Yamarna Terrane, Yilgarn Craton. Wacke and lithic sandstones, siltstone, abundant chert and banded iron-formation; felsic volcanic rocks; local intrusive rocks; metamorphosed.||||||
75926|Tobin Formation|68107|4|Described|p608 Fig.4, p614.|||Yamarna-Mount Gill Greenstone Belt, Yamarna Terrane.||||Overlies, and locally intercalated with, Toppin Hill Formation.|Comprises wacke, lithic sandstones, siltstones, minor volcaniclastic rocks; ferruginous banded chert, and banded iron-formation.|
75926|Tobin Formation|68186|5|Briefly described|Plates 1A, 2|Archean|Archean|Yamarna Terrane, Yilgarn Craton.|||||Wacke, lithic sandstone, siltstone, abundant chert and BIF, and minor felsic volcaniclastic rocks; metamorphosed.|
75926|Tobin Formation|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yamarna Terrane, Eastern Goldfields Superterrane, Yilgarn Craton.|||Includes 3 unnamed subunits.||Wacke, lithic sandstone, siltstone, abundant chert and banded iron-formation, and minor felsic volcaniclastic rocks; metamorphosed.|07-AUG-15
75926|Tobin Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|See also 100k_geologyp14_lut.csv. Age derived from psammitic schist sample (182314.1.pdf) and constrains maximum age of deposition of the sedimentary protolith. 2682-2640 Ma inferred age range.|2686 +/- 4 Ma (SHRIMP)||||Wacke, lithic sandstone, siltstone, abundant chert and banded iron-formation, and minor felsic volcaniclastic rocks; metamorphosed.|
75926|Tobin Formation|70802|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yamarna Terrane, Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Tropicana Event (2520-2505 Ma); Eastern Goldfields Superterrane events (2960-2600 Ma); Yilgarn Craton granite magmatism (3010-2600 Ma). See 500k_interpgeop14_lut.csv, 250k_pre_mesozoic_interpgeop_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|2682-2640 Ma (inferred)||||Wacke, lithic sandstone, siltstone, abundant chert and banded iron-formation, and minor felsic volcaniclastic rocks; metamorphosed|
75926|Tobin Formation|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yamarna Terrane, Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Tropicana Event (2520 - 2505 Ma); Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma). Sample GSWA 182314 (psammitic schist) yielded a weighted mean 207Pb/206Pb date of 2663+\-11 Ma, interpreted as the maximum depositional age of the sedimentary protolith of the schist. See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 100k_geologyp14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 100k_geologysub14_lut.csv, 2_5m_interpgeop15_lut.csv, 100k_geologyl14_lut.csv.|2682-2640 Ma (inferred)|||Underlain by and locally interleaved with Toppin Hill Formation.|Wacke, lithic sandstone, siltstone, abundant chert and banded iron-formation, and minor felsic volcaniclastic rocks; metamorphosed|
75926|Tobin Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||||||Wacke, lithic sandstone, siltstone, abundant chert and banded iron-formation, and minor felsic volcaniclastic rocks; metamorphosed.|
31059|Toby Gabbro|22754|6|Mentioned|p7|||||||||
31059|Toby Gabbro|23751|4|Described|p9|Orosirian|Orosirian|Age: 1855+/-2 Ma (SHRIMP U-Pb zircon).||||||
31059|Toby Gabbro|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
31059|Toby Gabbro|43854|5|Briefly described|Map Legend||Proterozoic|||||||
31059|Toby Gabbro|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
31059|Toby Gabbro|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31059|Toby Gabbro|50437|6|Mentioned|p3.4|||||||||
31059|Toby Gabbro|64580|6|Mentioned|map legend|||Of Paperbark Supersuite.||||||15-DEC-08
31059|Toby Gabbro|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Paperbark Supersuite|||Fine-grained, sub-ophitic, biotite- and quartz-bearing gabbro and gabbronorite.|04-AUG-15
31059|Toby Gabbro|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Paperbark Supersuite|||Fine grained, sub-ophitic, biotite and quartz bearing gabbro and gabbronorite.|
31059|Toby Gabbro|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone.|1855-1855 Ma (Isotopic)|Unit of Paperbark Supersuite.|||Fine-grained, sub-ophitic, biotite- and quartz-bearing gabbro and gabbronorite|
31059|Toby Gabbro|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1855 Ma|Paperbark Supersuite|||Fine grained, sub-ophitic, biotite and quartz bearing gabbro and gabbronorite.|
31059|Toby Gabbro|70731|6|Mentioned|p274,279|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. Mafic-ultramafic intrusion.|c. 1850 Ma|||||
31059|Toby Gabbro|70812|5|Briefly described|p6, p8, p20, p22, p43|Orosirian|Orosirian|Western Zone of the Halls Creek Orogen, Lamboo Province. No mineral deposits are known in this unit.|c. 1855 Ma||||Mafic magmatics.|
31059|Toby Gabbro|70851|5|Briefly described|p4, p16|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province. Geophysical response is discussed.  |c. 1850 Ma|||||
31059|Toby Gabbro|71267|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (183 -1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma)|1855+\-2 Ma (isotopic)|Unit of Paperbark Supersuite.|||Fine-grained, sub-ophitic, biotite- and quartz-bearing gabbro and gabbronorite|
23017|Togo Monzogranite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.||||||07-NOV-08
23017|Togo Monzogranite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1850Ma. Geological province: Kimberley Province (East).||||||07-FEB-11
23017|Togo Monzogranite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
23017|Togo Monzogranite|43854|5|Briefly described|Map Legend||Proterozoic|||||||
23017|Togo Monzogranite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
23017|Togo Monzogranite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite.||||||07-NOV-08
23017|Togo Monzogranite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Paperbark Supersuite|||Foliated, medium- to coarse grained, porphyritic biotite metamonzogranite and minor metagranodiorite.|04-AUG-15
23017|Togo Monzogranite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Paperbark Supersuite|||Foliated, medium to coarse grained porphyritic biotite-hornblende monzogranite.|
23017|Togo Monzogranite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone.|1864-1852 Ma (Inferred)|Unit of Paperbark Supersuite.|||Foliated, medium- to coarse grained, porphyritic biotite metamonzogranite and minor metagranodiorite|
23017|Togo Monzogranite|70154|6|Mentioned|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1852-1864 Ma|Paperbark Supersuite||||
23017|Togo Monzogranite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (183 -1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1864-1852 Ma (inferred)|Unit of Paperbark Supersuite.|||Moderately to strongly foliated, medium- to coarse-grained, porphyritic biotite monzogranite and minor granodiorite|
23017|Togo Monzogranite|72437|5|Briefly described|p84-85|||Lamboo Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Foliated porphyritic biotite monzogranite.|
79176|Toolgana Supersuite|70831|5|Briefly described|p25-p26|Statherian|Statherian|Coompana Province.|c. 1613-1604 Ma|||||
79176|Toolgana Supersuite|71143|5|Briefly described|p427,429,431-432,435-437,440|Statherian|Statherian|Geological province: Coompana Province. Oldest rocks in the Eucla basement region. Contains chemical and isotopic characteristics of primitive arc rock. Calc-alkaline suite; geochemical analysis indicate a subduction origin or re-melting of a subduction-derived source, or incorporation of crustal material into a mantle-derived melt. No known rocks equivalent in age to the Toolgana Supersuite in the Madura Province.|c. 1610 Ma||||Foliated feldspar-porphyritic granites interleaved with medium-grained monzodiorite and rare monzogabbro.|
79176|Toolgana Supersuite|71165|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Eastern Coompana Province.|c.1613 Ma.||||Granitic and mafic gneiss.|
79176|Toolgana Supersuite|71169|5|Briefly described|p77|Statherian|Statherian|Coompana Province. Features arc-like geochemistry (Smithies et al., 2015b).|1613-1604 Ma (Wingate et al., 2015)||||Calc-alkaline granitic gneiss.|
79176|Toolgana Supersuite|71618|6|Mentioned|p133|Statherian|Statherian|Geological province: Coompana Province. Possible source of c~1500-1800 Ma detrital zircons in the Madura Formation, Loongana Formation and Decoration Sandstone.|c. 1610 Ma||||Granites and monzogranite.|
79176|Toolgana Supersuite|71891|5|Briefly described|p7, p30, p33-p34|||Coompana Province. See also p38-p40, p47, p49, p51-p52, p55.|c. 1610 Ma||||Migmatitic monzodioritic to granodioritic to monzogranitic gneiss and metadolerites.|
79176|Toolgana Supersuite|72242|5|Briefly described|p27,29-30|Calymmian|Statherian|Geological province: Musgrave Province. Associated with Kararan Orogeny. Coeval with Hiltaba Suite and Birksgate Complex, and extensive oceanic crust formation.|||Includes Koomalboogurra Suite.|||
79176|Toolgana Supersuite|72344|6|Mentioned|p3, p5, p7-p9, p16-p17, p28|Statherian|Statherian|Coompana Province. The same age as, and geochemically and isotopically similar to the St Peter Suite. Previously identified in drillcore from the Forrest Zone and Kutjara 1. Granites of this supersuite have protolith ages of c. 1591-1613 Ma. A magmatic age of 1614 +/- 12 Ma is derived via SHRIMP. Basement in CDP001 is assigned to this unit. Petrography, SHRIMP analyses and geochemistry are discussed for several samples. See also p96, p98, p102, p143, p169.|c. 1610-1620 Ma||Includes the Koomalboogurra Suite|Time equivalent of the St Peter Suite and Birksgate Complex.||04-SEP-19
79176|Toolgana Supersuite|72465|5|Briefly described|p4, 10, 17|||Spaggiari and Smithies (2015). Coompana Province. Product of arc magmatism and recycling of oceanic crust. Metamorphic ages range from 1179 +/- 10 Ma to 1150 +/- 10 Ma. Is similar geochemically, isotopically and in age to the St Peter Suite (western Gawler Craton). Basement lithologies described in detail; photos of core.|1613 +/- 13 Ma to 1591 +/- 11 Ma.|||Is overlain by Madura Formation.|Locally migmatitic monzodioritic to granodioritic to monzogranitic gneisses and metadolerites that have been metamorphosed to amphibolite facies.|
79176|Toolgana Supersuite|72466|5|Briefly described|p4, 10|||Spaggiari and Smithies (2015). Basement to Coompana Province. Metamorphosed between 1179 +/- 10 Ma and 1150 +/- 10 Ma. Derived from a mantle wedge or subduction-modified lithosphere. Has the same age, and similar geochemistry and isotopes, as St Peter Suite in western Gawler Craton.|1613/- 13 Ma to 1591 +/- 11 Ma.||||Locally migmatitic monzodioritic to granodioritic to monzogranitic gneisses and metadolerites that have been metamorphosed to amphibolite facies.|
79176|Toolgana Supersuite|72467|5|Briefly described|p4, 10|||Spaggiari and Smithies (2015). Coompana Province. Product of arc magmatism and recycling of oceanic crust. Metamorphic ages range from 1179 +/- 10 Ma to 1150 +/- 10 Ma. Is similar geochemically, isotopically and in age to the St Peter Suite (western Gawler Craton). Basement lithologies described in detail; photos of core.|1613/- 13 Ma to 1591 +/- 11 Ma.|||Is overlain by Madura Formation.|Locally migmatitic monzodioritic to granodioritic to monzogranitic gneisses and metadolerites that have been metamorphosed to amphibolite facies.|
79176|Toolgana Supersuite|72468|5|Briefly described|p4, p10, p13, p17|Statherian|Statherian|Coompana Province. Represents arc magmatism and recycling of oceanic crust. Same age as, and is geochemically and isotopically similar to St Peter Suite. Magmatic ages include 1613 +/- 4 Ma, 1611 +/- 7 Ma, 1613 +/- 13 Ma, 1604 +/- 6 Ma, and 1591 +/- 11 Ma. Metamorphic ages include 1179 +/- 10 Ma, 1150 +/- 10 Ma, and 1167 +/- 7 Ma.|c. 1610 Ma||||Granitic to monzodioritic rocks including locally migmatitic monzodioritic to granodioritic to monzogranitic gneisses and metadolerites that have been metamorphosed to amphibolite facies.|
79176|Toolgana Supersuite|72469|5|Briefly described|p4, p10|Statherian|Statherian|Coompana Province. Represents arc magmatism and recycling of oceanic crust. Same age as, and is geochemically and isotopically similar to St Peter Suite. Magmatic ages include 1613 +/- 4 Ma, 1611 +/- 7 Ma, 1613 +/- 13 Ma, 1604 +/- 6 Ma, and 1591 +/- 11 Ma. Metamorphic ages include 1179 +/- 10 Ma, 1150 +/- 10 Ma, and 1167 +/- 7 Ma.|c. 1610 Ma||||Granitic to monzodioritic rocks including locally migmatitic monzodioritic to granodioritic to monzogranitic gneisses and metadolerites that have been metamorphosed to amphibolite facies.|
79176|Toolgana Supersuite|72470|5|Briefly described|p4, p10, p13, p18|Statherian|Statherian|Coompana Province. Represents arc magmatism and recycling of oceanic crust. Same age as, and is geochemically and isotopically similar to St Peter Suite. Magmatic ages include 1613 +/- 4 Ma, 1611 +/- 7 Ma, 1613 +/- 13 Ma, 1604 +/- 6 Ma, and 1591 +/- 11 Ma. Metamorphic ages include 1179 +/- 10 Ma, 1150 +/- 10 Ma, and 1167 +/- 7 Ma.|c. 1610 Ma||||Granitic to monzodioritic rocks including locally migmatitic monzodioritic to granodioritic to monzogranitic gneisses and metadolerites that have been metamorphosed to amphibolite facies.|
79176|Toolgana Supersuite|72471|5|Briefly described|p4, p10|Statherian|Statherian|Coompana Province. Represents arc magmatism and recycling of oceanic crust. Same age as, and is geochemically and isotopically similar to St Peter Suite. Magmatic ages include 1613 +/- 4 Ma, 1611 +/- 7 Ma, 1613 +/- 13 Ma, 1604 +/- 6 Ma, and 1591 +/- 11 Ma. Metamorphic ages include 1179 +/- 10 Ma, 1150 +/- 10 Ma, and 1167 +/- 7 Ma.|c. 1610 Ma||||Granitic to monzodioritic rocks including locally migmatitic monzodioritic to granodioritic to monzogranitic gneisses and metadolerites that have been metamorphosed to amphibolite facies.|
79176|Toolgana Supersuite|72472|5|Briefly described|p4, p10|Statherian|Statherian|Coompana Province. Represents arc magmatism and recycling of oceanic crust. Same age as, and is geochemically and isotopically similar to St Peter Suite. Magmatic ages include 1613 +/- 4 Ma, 1611 +/- 7 Ma, 1613 +/- 13 Ma, 1604 +/- 6 Ma, and 1591 +/- 11 Ma. Metamorphic ages include 1179 +/- 10 Ma, 1150 +/- 10 Ma, and 1167 +/- 7 Ma.|c. 1610 Ma||||Granitic to monzodioritic rocks including locally migmatitic monzodioritic to granodioritic to monzogranitic gneisses and metadolerites that have been metamorphosed to amphibolite facies.|
79176|Toolgana Supersuite|72934|5|Briefly described|p2, p4, p11-12, App.A|Statherian|Statherian|Interpreted to be derived from a subduction-enriched mantle source, compatible with a primitive arc setting. Yielded U-Pb SIMS zircon magmatic crystallisation ages of 1618 +/- 6 Ma and 1618 +/- 9 Ma; a metamorphic age of 1163 +/- 8 Ma; and an inheritance age of c. 1720 Ma.|c. 1610 Ma||||Magnesian, calc-alkalic, high-K granitic to dioritic gneisses.|
79176|Toolgana Supersuite|72947|5|Briefly described|p4, p7-9, p12|Calymmian|Statherian|Coompana Province. Represents arc magmatism.|c. 1610 Ma / 1622 - 1591 Ma||Koomalboogurra Suite|Sheared contact with Bunburra Suite.||29-NOV-22
79176|Toolgana Supersuite|73084|4|Described|p: 12, 15, 32, 34, 44-45, 69-70, 72...|Statherian|Statherian|Coompana Province. Biranup Orogeny. Oldest rocks sampled in the Coompana Province. Upper amphibolite to granulite facies. Most likely subduction related; intruded c. 1724 to 1671 Ma or older crust. May represent westward-migrating arcs. Possibly a regionally extensive, primitive arc-related suite, based also on similarities with the St Peter Suite, where subduction may have been directed towards the Gawler Craton margin. Metamorphism is dated at 1179 +/- 10, 1153 +/- 9 and 1151 +/- 6 Ma. Report includes lithologic/petrographic description, structural analysis, whole-rock geochemistry, geochronology, Sm-Nd, Lu-Hf. Also p: 100-116, ~123-129, ~133-137, 142.|1613-1604 Ma||Koomalboogurra Suite||Granite gneiss, and locally, diorite to amphibolite gneiss. Includes monzodiorite, granodiorite to monzogranite gneiss.|
79176|Toolgana Supersuite|73091|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic||||Includes Koomalboogurra Suite.|||
79176|Toolgana Supersuite|73224|5|Briefly described|p42, p44|Statherian|Statherian|Coompana Province, central. Underwent high-temperature anatexis at c. 1179-1150 Ma.|c. 1618-1604 Ma|||||
79176|Toolgana Supersuite|73225|5|Briefly described|p2, 4, 10, 18, p22 Fig.10|||Coompana Province. East of the Mulyawarra Shear Zone. Arc-related rocks; underwent high-T metamorphism and anatexis c.1179-1150 Ma. Age range also given as 1613-1604 Ma.|1618-1604 Ma.||Koomalboogurra Suite.||Migmatites.|
79176|Toolgana Supersuite|73641|6|Mentioned|p4||||||Koomalboogurra Suite|||
79474|Tooloo Group|69003|5|Briefly described|p4, p13 Fig.17, p14|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin, Capricorn Orogen. Fluvial to mainly shallow-marine deposits.|||Yelma, Frere Formations.|Is overlain unconformably by Miningarra Group.||
79474|Tooloo Group|69596|5|Briefly described|p4, p10-11, p32-34|Paleoproterozoic|Paleoproterozoic|Capricorn Orogen. Conductivity discussed.|||Yelma, Frere Formations.|Is overlain disconformably by Miningarra Group.|Shallow-marine sandstone and siltstone, granular iron-formation, and carbonate rocks.|
79474|Tooloo Group|70153|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin. Is listed as Tooloo Subgroup in 100k_geologyp10_lut.csv.|2027 +/- 23 Ma - 1600 Ma (inferred).||Includes Frere Formation, Yelma Formation.||Siltstone, sandstone, granular iron formation, and dolomite.|
79474|Tooloo Group|70795|5|Briefly described|2_5m_interpgeop15_lut.csv|Paleoproterozoic|Paleoproterozoic|500k_interpgeop14_lut.csv|2027-1650 Ma||||Siltstone, sandstone, granular iron formation and dolomite.|
79474|Tooloo Group|70826|6|Mentioned|p6 tbl 2, p9|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin. Time equivalent to the Camel Hills Metamorphics. ||||Overlain by the Miningarra Group.||
79474|Tooloo Group|71158|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin.|1971-1949 Ma.||Yelma Formation.|||
79474|Tooloo Group|71468|5|Briefly described|p26|||Geological province: Capricorn Orogen, Yilgarn Craton. Of Earaheedy Basin. Maximum depositional age at 1990+\-6 Ma (Nelson, 2001; Pirajno et al., 2009; Sheppard et al., 2016).||||Underlain by Mooloogool Group.||
79474|Tooloo Group|71484|4|Described|p122-125,130-132,135,137,139|Orosirian|Orosirian|Geological province:Of Earaheedy Basin. Nomenclature by Martin et al., 2016; Sheppard et al., 2016; replacing now obsolete Earaheedy Group, and Tooloo Subgroup. Partly coeval with Glenburgh Orogeny. Interpreted maximum age of c. 1996 Ma. Records a shallow marine trangression over the Yilgarn Craton. Interpreted to be partly coeval with lower Padbury Group and the sedimentary protoliths to Camel Hills Metamorphics.|1980-1940 Ma||Includes Frere Formation, Yelma Formation and Sweetwaters Well Dolomite.|Underlain unconformably by Mooloogool Group/Maraloou Formation.|Volcanosedimentary siliciclastics, carbonates and evaporites.|30-AUG-19
79474|Tooloo Group|71798|6|Mentioned|p110|||Earaheedy Basin.|||Includes the Frere Formation and the Yelma Formation.|||
79474|Tooloo Group|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin.|Max age 2027+/-23 Ma, min ~1650 Ma.||Includes Frere Formation, Yelma Formation.||Siltstone, sandstone, granular iron-formation, dolomite, chert.|
68632|Toorare Tonalite|63441|2|Defined|p10 Tb. 2, p37|Archean|Archean|Of the Maitland River Supersuite. Unconformably overlain by Hardey Formation. Intruded by Cherratta granitic Complex.  Age: 2995+/-11Ma. Geological province: Pilbara Craton. Distinctive magnetic unit characterised by hornblende phenocrysts.||||||07-FEB-11
68632|Toorare Tonalite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Maitland River Supersuite. Geological province: Pilbara Craton.  Hornblende metatonalite and metagranodiorite; foliated and locally gneissic.||||||07-NOV-08
68632|Toorare Tonalite|64580|4|Described|map legend||Mesoarchean|Of Maitland River Supersuite. Hornblende metatonalite and metagranodiorite; foliated and locally gneissic.||||||15-DEC-08
68632|Toorare Tonalite|67201|4|Described|p16-17 Fig.9|Archean|Archean|Pilbara Craton. In Roebourne-Karratha area.||Maitland River Supersuite|||Hornblende metatonalite and metagranodiorite; foliated and locally gneissic.|
68632|Toorare Tonalite|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Maitland River Supersuite.|||Hornblende metatonalite and metagranodiorite; foliated and locally gneissic|
68632|Toorare Tonalite|70775|5|Briefly described|p15, p53-p54|||Pilbara Craton. Later intrusion has been dated at c. 2994 Ma (Nelson, 1997k). Good sections of this unit are exposed between Toorare Pool and Old Cherratta Homestead. Together with the Jean Well Granodiorite, Whyjabby Granodiorite, Brill Monzogranite, Waloo Waloo Monzogranite and Mardeburra Granodiorite comprises the Cherratta Granitic Complex.|c. 2995 to 2985 Ma (Smith, 2003)|Maitland River Supersuite|||Hornblende metatonalite and metagranodiorite; folaited and locally gneissic.|
68632|Toorare Tonalite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||tonalite, granodiorite|
68632|Toorare Tonalite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|De Grey Superbasin.|2995+/-11 Ma.|Maitland River Supersuite|||Hornblende metatonalite and metagranodiorite; foliated and locally gneissic.|
25545|Top Flag Sandstone|41170|6|Mentioned|p154|||||||||
31889|Top Water Tonalite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.||||||07-NOV-08
31889|Top Water Tonalite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1850Ma. Geological province: Kimberley Province (East).||||||07-FEB-11
31889|Top Water Tonalite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
31889|Top Water Tonalite|43854|5|Briefly described|Map Legend||Proterozoic|Of Paperbark supersuite.||||||
31889|Top Water Tonalite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31889|Top Water Tonalite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite.||||||07-NOV-08
31889|Top Water Tonalite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Paperbark Supersuite|||Medium-grained, quartz-phyric biotite tonalite and granodiorite; metasedimentary rock inclusions are abundant near contacts with Marboo Formation.|04-AUG-15
31889|Top Water Tonalite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Paperbark Supersuite|||Medium-grained, quartz-phyric biotite tonalite and granodiorite; metasedimentary rock inclusions are abundant near contacts with Marboo Formation.|
31889|Top Water Tonalite|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone. See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|1864-1854 Ma (Inferred)|Unit of Paperbark Supersuite.|||Medium-grained, quartz-phyric biotite tonalite and granodiorite; metasedimentary rock inclusions are abundant near contacts with Marboo Formation|
31889|Top Water Tonalite|70154|4|Described|100k_interpgeol_lut.csv|||||Paperbark Supersuite|||Medium grained, quarts phyric biotite tonalite and granodiorite; metasedimentary rock inclusions are common near contacts with Marboo Formation|
31889|Top Water Tonalite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (183 -1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 100k_interpgeol_lut.csv.|1864-1852 Ma (inferred)|Unit of Paperbark Supersuite.|||Medium-grained, quartz-phyric biotite tonalite and granodiorite; metasedimentary rock inclusions are abundant near contacts with Marboo Formation|
31889|Top Water Tonalite|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen, North Australian Craton.||Paperbark Supersuite.|||Medium-grained, quartz-phyric biotite tonalite and granodiorite; metasedimentary rock inclusions are abundant near contacts with Marboo Formation.|
31889|Top Water Tonalite|72437|5|Briefly described|p81-83|||Lamboo Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Biotite-granodiorite, foliated porphyritic biotie granodiorite and crenulated biotite granodiorite.|
75357|Toppin Hill Formation|66120|5|Briefly described|Map legend|Archean|Archean|Yamarna Terrane, Yilgarn Craton. Felsic schist; metamorphosed volcanics including dacite, rhyodacite, rhyolite (aged c.2699 Ma), felsic volcanic and volcaniclastic rocks (aged c.2682 Ma); minor sandstone to siltstone. ||||||
75357|Toppin Hill Formation|66121|5|Briefly described|Map legend|Archean|Archean|Yamarna Terrane, Yilgarn Craton. Felsic schist; metamorphosed volcanic and sedimentary rocks including dacite, rhyodacite, rhyolite (aged c.2683 Ma), felsic volcanic and volcaniclastic rocks; minor sandstone to siltstone. ||||||
75357|Toppin Hill Formation|68107|4|Described|p607 Fig.3, p608 Fig. 4, p609 Tb.1, p617|Neoarchean|Neoarchean|Of Romano et al (2010). Yamarna-Mount Gill Greenstone Belt, Yamarna Terrane. Contains xenocrysts dated at c. 2731 Ma (Wingate et al. 2011). A distinct lens-shaped concordant body, up to 3km thick and almost 30km long.|2683 +/- 5 Ma; 2677 +/- 7 Ma|||Overlain by, and locally intercalated with, the Tobin Formation.|Rhyolitic to andesitic, commonly quartz- and feldspar-phyric, volcanic and volcaniclastic rocks, with minor beds of siliciclastic sedimentary rock units.|22-SEP-14
75357|Toppin Hill Formation|68108|6|Mentioned|p652|Neoarchean|Neoarchean|Yamarna Terrane, Eastern Goldfields Superterrane.|ca. 2683 Ma (Pawley et al. 2012)||||Concurrent volcanic-granite magmatism.|
75357|Toppin Hill Formation|68186|5|Briefly described|Plates 1A, 2|Archean|Archean|Yamarna Terrane, Yilgarn Craton.|2699-2682 Ma (Sircombe et al., 2007).||||Felsic volcanic and volcaniclastic rocks, with minor siliciclastic sedimentary rocks; metamorphosed.|
75357|Toppin Hill Formation|69091|6|Mentioned|p31, p179|||Yamarna Terrane. Dated at c. 2699-2677 Ma (Sircombe et al., 2007; Wingate et al., 2011). Lu-Hf isotope data collected on a dacite (Pawley et al., 2012) also reveals substantial juvenile input, and average mantle extraction age of ~3000 Ma (Wyche et al., 2012).|SHRIMP magmatic crystallisation age 2677 +/- 7 Ma||||Felsic volcanics.|07-OCT-14
75357|Toppin Hill Formation|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yamarna Terrane, Eastern Goldfields Superterrane, Yilgarn Craton.|||Includes 7 unnamed subunits.||Sandstone, siltstone; andesite; dacite, rhyodacite; commonly feldspar-phyric; quartz- and feldspar-phyric dacite; felsic volcaniclastic and volcanic rocks; rhyolite; all metamorphosed.|07-AUG-15
75357|Toppin Hill Formation|69404|6|Mentioned|p4 Fig.4 |Neoarchean|Neoarchean|Yamarna Terrane|c. 2700 Ma|||||
75357|Toppin Hill Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|See also 100k_geologyp14_lut.csv and 500k_interpgeop14_lut.csv. Age dervied from metadacite sample (183150.1.pdf). Another age of 2683 +/- 5 Ma is determined; age range of 2699 Ma - 2677 Ma is inferred.|2677 +/- 7 Ma (SHRIMP)||||Sandstone, siltstone, minor felsic volcaniclastic rocks, metamorphosed; felsic schist; andesite, minor dacite; dacite, rhyodacite, quartz and feldspar phyric dacite; felsic volcaniclastic and volcanic rocks, minor sandstone and siltstone; rhyolite.|
75357|Toppin Hill Formation|70802|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yamarna Terrane, Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Tropicana Event (2520-2505 Ma); Eastern Goldfields Superterrane events (2960-2600 Ma); Yilgarn Craton granite magmatism (3010-2600 Ma). See 500k_interpgeop14_lut.csv, 250k_pre_mesozoic_interpgeop_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 100k_geologysub14_lut.csv.|2699-2677 Ma (inferred)||||Felsic volcanic and volcaniclastic rocks, with minor siliciclastic sedimentary rocks; metamorphosed|
75357|Toppin Hill Formation|70826|6|Mentioned|p9|Neoarchean|Neoarchean|Yamarna Terrane.||||||
75357|Toppin Hill Formation|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yamarna Terrane, Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Tropicana Event (2520 - 2505 Ma); Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma). Exposed in the central part of the Yamarna-Mount Gill greenstone belt in the Yarmarna Terrane (Pawley at al., 2009). Sircombe et al. (2007) reported an igneous crystallisation age of 2699+\-5 Ma for a metarhyolite. Sample GSWA 183150 (metadacite) yielded a concordia age of 2677+\-7 Ma, interpreted as the crystallisation age of the dacite. See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 100k_geologyp14_lut.csv, 500k_interpgeop_lut.csv, 100k_geologysub14_lut.csv, 2_5m_interpgeop15_lut.csv.|2699-2677 Ma (inferred)|||Overlain by and locally interleaved with Tobin Formation.|Andesite, dacite, quartz- and feldspar-phyric dacite, rhyodacite; metamorphosed, felsic volcanic and volcaniclastic rocks, sandstone, siltstone, rhyolite; metamorphosed.|
75357|Toppin Hill Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||||||Felsic volcanic and volcaniclastic rocks, with minor siliciclastic sedimentary rocks; metamorphosed.|
75357|Toppin Hill Formation|73453|5|Briefly described|p3|Neoarchean|Neoarchean|Yamarna Terrane.|2700-2675 Ma||||Felsic volcanics.|
25546|Torbay Adamellite|33274|3|Fully described|p228|||Metamorphic facies, structural relations etc.||||||
74826|Tough Go Monzogranite|64891|5|Briefly described|p37 Fig. 2, p42, p50-51 Tb. 1|Archean|Archean|Of Big Bell Suite (Austin Downs Supersuite). Age: 2710+/-10Ma. Geological province: Murchison Domain. Cuts across greenstones. Monzogranite, commonly foliated; metamorphosed.||||||07-FEB-11
74826|Tough Go Monzogranite|67129|5|Briefly described|p19 Fig.20|Archean|Archean|Murchison Domain, Youanmi Terrane.||Big Bell Suite.|||Late-volcanic granite.|
74826|Tough Go Monzogranite|69583|6|Mentioned|p52|||Murchison Domain.||||||
74826|Tough Go Monzogranite|70030|5|Briefly described|p191|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton.||Unit of Big Bell Suite.||||
74826|Tough Go Monzogranite|70830|6|Mentioned|p8|||Murchison Domain. ||||||
74826|Tough Go Monzogranite|73410|5|Briefly described|p4-5|||Youanmi Terrane. Appears as Tough Go monzogranite on p4.|2710 +/- 10 Ma (Wang et al., 1995).||||Synorogenic granitic pluton. Undeformed.|
74826|Tough Go Monzogranite|73596|6|Mentioned|p1160|Neoarchean|Neoarchean|Kalgoorlie Terrane. Presented as the informal Tough Go monzogranite.|2710 +/- 10 Ma.|||||
23033|Toweranna Porphyry|23793|5|Briefly described|p34|Archean|Archean|Age: c.2954+/-4Ma.||||||07-NOV-08
23033|Toweranna Porphyry|23794|5|Briefly described|Map Legend|Archean|Archean|Geological Province Pilbara Craton.||||||07-NOV-08
23033|Toweranna Porphyry|43821|5|Briefly described|map legend|Archean|Archean|Possibly equivalent to Peawah Granodiorite.||||||07-NOV-08
23033|Toweranna Porphyry|63441|5|Briefly described|p11 Tb. 2|Archean|Archean|Of Indee Suite (Sisters Supersuite). Geological province: Pilbara Craton. Intrudes De Grey Supergroup.||||||07-FEB-11
23033|Toweranna Porphyry|64580|4|Described|map legend||Mesoarchean|Of Indee Suite. Porphyritic high-Mg granodiorite; metamorphosed.||||||09-DEC-08
23033|Toweranna Porphyry|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Indee Suite.|||Porphyritic high-Mg granodiorite; metamorphosed|
23033|Toweranna Porphyry|69300|5|Briefly described|map legend|Archean|Archean|Mallina Basin|||||Metamorphosed porphyritic high-Mg granodiorite.|03-SEP-14
23033|Toweranna Porphyry|70775|6|Mentioned|p65|||||Indee Suite||||
25549|Town Dam ophiolites|36869|6|Mentioned|p48|||||||||
31018|Tozer Formation|23484|4|Described|p10 table 3|Archean|Archean|Of Whundo Group.  Maximum thickness: 2500m.||||||07-NOV-08
31018|Tozer Formation|23784|5|Briefly described|p10|Archean|Archean|Of Whundo Group.||||||07-NOV-08
31018|Tozer Formation|23789|5|Briefly described|p9 Tb. 2|Archean|Archean|Parent: Whundo Group. Max. Thickness: 2500m. Age: c.3120Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
31018|Tozer Formation|23793|4|Described|p16|Archean|Archean|Of Whundo Group. Thickness: 2500m.  See also page 11 table 2 Age: ~3120Ma||||||07-NOV-08
31018|Tozer Formation|23794|5|Briefly described|Map Legend|Archean|Archean|Of Whundo Group. Overlain by Bradley Basalt. Underlain by Nallana Formation. Geological Province: Pilbara Craton.||||||07-NOV-08
31018|Tozer Formation|24023|5|Briefly described|p7 fig. 4|Archean|Archean|Of Whundo Group. Maximum thickness: 2500m.||||||07-NOV-08
31018|Tozer Formation|24184|4|Described|p712 Tb.3|Archean|Archean|Of the Whundo Group. Overlain by Bradley Basalt. Underlain by Nallana Formation. Geological Province: Pilbara Craton. Max Thickness: 2500m. Age: 3120Ma||||||07-NOV-08
31018|Tozer Formation|24353|4|Described|p9 Fig.5, p11 Tb.2|Archean|Archean|Parent: Whundo Group. Age: c.3120Ma. Max Thickness: 2500m. Geological Province: Pilbara Craton||||||07-NOV-08
31018|Tozer Formation|24541|3|Fully described|p11 Tb.2, p23|Archean|Archean|Of the Whundo Group. Age: c. 3120 Ma. Maximum Thickness: 2500m. Conformably overlies the Nallana Formation.||||||07-NOV-08
31018|Tozer Formation|24543|5|Briefly described|Map legend|Archean|Archean|Of the Whundo Group (Pilbara Supergroup).  Age: c. 3120Ma.  Felsic volcanic rock, basalt and andesite.||||||07-NOV-08
31018|Tozer Formation|24550|5|Briefly described|p36 Tb. 3.2|Archean|Archean|Of the Whundo Group. Consists of a range of extrusives from basalt to rhyolite, and minor sediments and chert.Overlies the Nallana Formation.  Age: ca 3120Ma. Thickness: 2.5km. See also p39.||||||07-FEB-11
31018|Tozer Formation|50430|5|Briefly described|p163||Archean|Felsic volcanics in Whundo Group.||||||07-NOV-08
31018|Tozer Formation|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Age: ~3.1Ga.   Geological Province: Pilbara Craton.||||||07-NOV-08
31018|Tozer Formation|63372|4|Described|Map Legend|Archean|Archean|Of the Whundo Group. Geological Province: West Pilbara Granite-Greenstone Terrane. Age: 3120Ma. Mafic and felsic lava and pyroclastic units; metamorphosed.||||||07-NOV-08
31018|Tozer Formation|63441|4|Described|p5 Tb.1, p24|Archean|Archean|Of Whundo Group.Conformable on Nallana Fm; conformable below Bradley Basalt. Age: c.3126Ma and 3118Ma. Thick: 2500m.Geol.prov: West Pilbara Superterrane. Alternating metamorphosed basalt, andesite, dacite, rhyolite + thin sed.units including chert and BIF.||||||01-JUL-14
31018|Tozer Formation|63538|5|Briefly described|p6 Fig. 3|Archean|Archean|Of Whundo Group. Overlain by Bradley Basalt, underlain by Nallana Formation. Geological Province: Pilbara Craton.||||||19-APR-13
31018|Tozer Formation|64174|5|Briefly described|Map legend|Archean|Archean|Of the Whundo Group. Age: 3128-3118Ma. Basalt and dacitic to rhyolitic lava and pyroclastic rocks; variable silicification and carbonate alteration; metamorphosed.||||||07-NOV-08
31018|Tozer Formation|64580|4|Described|map legend||Mesoarchean|Of Whundo Group. Basalt and dacitic to rhyolitic lava and pyroclastic rocks, variable silicification and carbonate alteration; metamorphosed.||||||15-DEC-08
31018|Tozer Formation|64632|6|Mentioned|p203 Fig.2|||||Of the Whundo Group.||Underlain by the Nallana Formation. Overlain by the Bradley Basalt.||
31018|Tozer Formation|67201|4|Described|p7 Fig.4, p12 Tb.1, p15-18|Archean|Archean|In northwestern Pilbara Craton, West Pilbara Superterrane, Sholl Terrane, Whundo Basin. Thickness: 2.5 km.|c. 3120 Ma|Whundo Group||Conformably overlies Nallana Formation. Is conformably overlain by Bradley Basalt.|Basalt, andesite, and dacitic to rhyolitic lava and pyroclastic rocks; thin meta-sedimentary units; variable silicification and carbonate alteration; metamorphosed.|
31018|Tozer Formation|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological province: West Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 3120 Ma|Unit of Whundo Group.|||Basalt and dacitic to rhyolitic lava and pyroclastic rocks, variable silicification and carbonate alteration; metamorphosed|
31018|Tozer Formation|69299|5|Briefly described|p5 Fig.4, p6 Tb.1, p7, p11|Mesoarchean|Mesoarchean|Stratigraphically the lowest basalt (adjacent to Mount Roe Basalt) of Whundo Group (Hickman 1997). Thickness on COOYA POOYA: 2000 m. c. 3120 Ma volcanic-hosted massive sulphide Cu-Zn mineral deposits on PINDERI HILLS. The main basaltic rock of the Whundo Group. |c. 3120 Ma||||Felsic tuff; calc-alkaline volcanic rocks, including felsic pyroclastic units; minor chert and very thin banded iron-formation.|01-JUL-14
31018|Tozer Formation|69301|4|Described|p5 Fig.3, p9 Tb.1|||Pilbara Craton. West Pilbara Superterrane. Whundo Basin. Sholl Terrane. Thickness: 2.5 km.|3120 Ma|Whundo Group||Conformably overlies Nallana Formation. Is conformably overlain by Bradley Basalt.|Felsic volcanic rocks. Contains basalt, andesite, dacite, rhyolite, and thin metasedimentary units.|
31018|Tozer Formation|70022|6|Mentioned|p115|||West Pilbara Superterrane.||Whundo Group.||||
31018|Tozer Formation|70775|4|Described|p12, p15, p25 tbl 4, p32-p36, p41, p74|Mesoarchean||Whundo Basin. Also dated at 3128 +/- 7 Ma (Smith, 2003). This unit is 2500m thick. Lithology is broadly discussed.|c. 3128-3118 Ma|Whundo Group||Conformably overlies the Nallana Formation. Conformably overlain by the Bradley Basalt.|Basalt and dacitic to rhyolitic lava and pyroclastic rocks; variable silicification and carbonate alteration.|
31018|Tozer Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Whundo Basin.|Max age 3128+/-4 Ma, min 3118+/-3 Ma.|Whundo Group|||Basalt and dacitic to rhyolitic lava and pyroclastic rocks, variable silicification and carbonate alteration; metamorphosed.|
31018|Tozer Formation|72251|5|Briefly described|p54|Mesoarchean|Mesoarchean|Geological province: West Pilbara Superterrane, Pilbara Craton.||||Overlain by Bradley Basalt. Underlain by Nallana Formation.||
31018|Tozer Formation|72668|6|Mentioned|p4, p13|||West Pilbara Superterrane.||Whundo Group||Overlies the Nallana Formation. Overlain by the Bradley Basalt.||14-JAN-22
30171|Trafalgar Dolerite|43102|6|Mentioned|p8|||Of Devon Consols Basalt?||||||
30171|Trafalgar Dolerite|60623|5|Briefly described|p28|Archean|Archean|Of Devon Consols Basalt.||||||07-NOV-08
35919|Treachery Formation|13222|6|Mentioned|p229 Fig.2.|||Name replaced by Treachery Shale.||||||
35919|Treachery Formation|23356|5|Briefly described|26 Tab.2|Early Permian|Early Permian|||||||
35919|Treachery Formation|23377|6|Mentioned|p212 Fig.5||Pennsylvanian|In the Vulcan Sub-basin.||||||12-DEC-06
35919|Treachery Formation|60666|5|Briefly described|p15 (Fig.)|||Geological Province: Bonaparte  Basin.||||||
35919|Treachery Formation|67354|2|Defined|p74, p75, pp78-91. |Sakmarian|Sakmarian|Formerly Treachery Shale (Mory 1988). Reference section is proposed between 2,827.3 m MDRT and 3.072.8 m MDRT in Blacktip North-1. Shales in this unit act as seals for hydrocarbons in the Kuriyippi Formation. Oil and gas shows are often seen within sandstones in this unit. Trace fossils are sometimes abundant, but few are diagnostic for a marine environment. The palynology is discussed in detail. Has equivalents in Calytrix Formation (Canning Basin), upper Lyons Group (Carnarvon Basin), and Nangetty Formation (Perth Basin): all contain G. confluens Oppel Zone and evidence of ice-transported debris.|||Includes Blacktip Member.|Unconformably overlies Kuriyippi Formation.|Predominantly carbonaceous, argillaceous, tillitic and varved siltstone with claystone; minor sandstone; several cores have massive diamictic fabric with facetted pebbles.|
35919|Treachery Formation|69451|6|Mentioned|p35:9|||Bonaparte Basin. Correlated with part of the Kulshill Group equivalent rocks in the Arafura Basin.||||||12-JUL-16
35919|Treachery Formation|69452|4|Described|p36:9, 11, 15, 18-19|Sakmarian|Sakmarian|Mory (1988). Petrel Sub-basin, Bonaparte Basin. Subsurface. Glacigenic, marine at least in part, possibly marginal marine or non-marine. Over 300m thick. Offshore and onshore. Includes the informal Blacktip member.||Kulshill Group.||Unconformably overlies Border Creek and Kuriyippi Formations. Is overlain by Quoin Formation, probably unconformably.|Tillite, diamictite (containing exotic pebbles, some facetted), carbonaceous shale, varved siltstone, sandstone, and minor limestone and coal.|12-JUL-16
35919|Treachery Formation|69454|5|Briefly described|p38:4|Sakmarian|Sakmarian|Petrel Sub-basin, Bonaparte Basin.||Kulshill Group.||||12-JUL-16
35919|Treachery Formation|69653|6|Mentioned|p10|Cisuralian|Cisuralian|Petrel Sub-basin.||Kulshill Group.||Overlies Kuriyippi Formation. Is overlain by Quoin Formation.||
35919|Treachery Formation|69673|4|Described|p168 fig 139, p170 fig 142, p173|Permian|Carboniferous|||Kulshill Group||Overlain by Quoin Formation, Keyling Formation, overlies Kuriyippi Formation|Tillite, diamictite, carbonaceous shale, varved siltstone, sandstone and minor limestone and coal.|
35919|Treachery Formation|70061|5|Briefly described|Petrel Sub-basin Figs.2 & 3, p3|Sakmarian|Sakmarian|See also Regional geology: Fig.8, p5, p11. Hydrocarbon reservoir.||Kulshill Group.||Overlies Kuriyippi Formation. Is overlain by Quoin Formation.|Glacial sediments.|12-JUL-16
35919|Treachery Formation|71146|6|Mentioned|p44|||Southern Bonaparte Basin.||Kulshill Group||||
35919|Treachery Formation|72505|5|Briefly described|p890|Asselian|Asselian|Southern Bonaparte Basin. Correlatyed with the P. Confluens zone.||||Overlies the Kuriyippi Formation. Overlain by the Quoin Formation.||
35919|Treachery Formation|73117|6|Mentioned|p15|Asselian|Asselian|Bonaparte Basin, southern.||Kulshill Group||Underlain by Kuriyippi Formation. Overlain by Quoin Formation.||
79013|Trevors Bore Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||2817 - 2753 Ma (inferred).||||Basalt and komatiitic basalt; metamorphosed. Amphibolite; derived from mafic rock. Talc-serpentine-chlorite schist. Sandstone and siltstone; metamorphosed. Peridotite; relict olivine cumulate texture; commonly serpentinized; metamorphosed.|
79013|Trevors Bore Formation|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Mesoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2817-2753 Ma (inferred)||||Sandstone, siltstone, mafic amphibolite; foliated, lineated; basalt and komatiitic basalt; relict pyroxene spinifex texture; metamorphosed; talc-serpentine-chlorite schist; peridotite; relict olivine cumulate texture, serpentinised, metamorphosed.|
79013|Trevors Bore Formation|73596|6|Mentioned|p1159, 1162-1163, 1170|Neoarchean|Neoarchean|Leonora Inlier, Kalgoorlie-Kurnalpi Rift.|2750 Ma.|||Is overlain conformably by Mount Leonora Formation.|Mafic and ultramafic rocks: basalt, komatiite, BIF, chert, and interflow mudstone.|
36769|Triberton Granodiorite|50381|5|Briefly described|Map Legend|Archean|Archean|Of Corunna Downs Granitoid Complex. Geological Province: Pilbara Craton. Lithology: biotite-hornblende granodiorite to tonalite; medium to coarse grained, feldspar porphyritic; common mafic xenoliths; minor porphyritic monzogranite.||||||26-OCT-15
36769|Triberton Granodiorite|63441|5|Briefly described|p8 Tb. 2|Archean|Archean|Of Emu Pool Supersuite. Age: <3317Ma, <3300Ma. Geological province: Pilbara Craton.||||||07-FEB-11
36769|Triberton Granodiorite|64327|5|Briefly described|p63|Archean|Archean|Of Corunna Downs Granitoid Complex. Porphyrytic, medium- to coarse-grained, biotite-hornblende granodiorite with minor medium-grained tonalite and porphyritic monzogranite containing abundant mafic xenoliths.||||||26-OCT-15
36769|Triberton Granodiorite|65008|6|Mentioned|p12|||||Of the Corunna Downs Granitoid Complex||||
36769|Triberton Granodiorite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Emu Pool Supersuite. Feldspar porphyritic biotite-hornblende granodiorite to tonalite; medium- to coarse-grained; common mafic xenoliths; minor porphyritic monzogranite; weakly metamorphosed.||||||
36769|Triberton Granodiorite|69012|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Of the Emu Pool Supersuite.|||Comprises feldspar-porphyritic biotite-hornblende granodiorite to tonalite; medium to coarse grained; common mafic xenoliths; minor porphyritic monzogranite; weakly metamorphosed.|
36769|Triberton Granodiorite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Emu Pool Supersuite|||Feldspar porphyritic biotite--hornblende granodiorite to tonalite; medium to coarse grained; common mafic xenoliths; minor porphyritic monzogranite; weakly metamorphosed. Hornblende monzogranite with amphibolite xenoliths; weakly metamorphosed.|
36769|Triberton Granodiorite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3325-3277 Ma (inferred)|Unit of Emu Pool Supersuite.|||Feldspar porphyritic biotite-hornblende granodiorite to tonalite; medium to coarse grained; common mafic xenoliths; minor porphyritic monzogranite; weakly metamorphosed; and hornblende monzogranite with abundant amphibolite xenoliths.|
36769|Triberton Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||tonalite, granodiorite, monzogranite|
36769|Triberton Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|||Emu Pool Supersuite|||Biotite-hornblende granodiorite to tonalite; feldspar porphyritic; medium to coarse grained; common mafic xenoliths; weakly metamorphosed.|
39775|Trigg Hill pegmatite|24193|5|Briefly described|p877 Tb.1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
80089|Trillbar Formation|70795|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|Bryah Basin.|2014-1920 Ma inferred.|Bryah Group.|||Gabbro, microgabbro, mafic and ultramafic schist; minor mafic rock; metamorphosed.|25-SEP-17
80089|Trillbar Formation|70796|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|Bryah Basin, Capricorn Orogen.|2014  1920 Ma (inferred)|Bryah Group, lower|||Gabbro, microgabbro, mafic and ultramafic schist; minor mafic rock; metamorphosed.|
80089|Trillbar Formation|71269|4|Described|500k_interpgeop16_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen, West Australian Craton. Of Bryah Basin. Events: Capricorn Orogeny (1817-1772 Ma); Glenburgh Orogeny (2002-1947 Ma).|2014-1920 Ma (inferred)|Unit of Bryah Group.|||Gabbro, microgabbro, mafic and ultramafic schist; minor mafic rock; metamorphosed|
74816|Triton Tonalite|64891|5|Briefly described|p37 Fig. 2, p50-51 Tb. 1|Archean|Archean|Of Cullculli Suite (Annean Supersuite). Age: 2785Ma. Geological province: Murchison Domain. Metatonalite.||||||07-FEB-11
79293|Tropicana Gneiss|69743|5|Briefly described|p189-191, 193|Archean|Archean|Plumridge Terrane, Yilgarn Craton, Albany-Fraser Orogen. Hosts the Tropicana gold deposit. Metamorphosed at 2643 +/- 7 Ma; both age determinations by Spaggiari et al. (2011). Deformation history and structural controls on ore bodies.|2722 +/- 15 Ma (U-Pb zircon).|||Is intruded by the Gnowangerup-Fraser Dyke Suite.|Granulite facies quartzo-feldspathic gneisses: felsic gneiss, granulite, amphibolite, BIF.|
79293|Tropicana Gneiss|70089|5|Briefly described|p261, 263, 265, 272, 276|Archean|Archean|Tropicana Zone, Albany-Fraser Orogen. Hosts the Tropicana Au deposit. High-grade metamorphism at 2640 +/- 10 Ma.|2722 +/- 15 Ma (protolith).||||Amphibolite- to granulite-facies quartzofeldspathic gneiss, garnet-bearing gneiss, mafic to ultramafic gneiss, metachert, and meta-iron formation.|
79293|Tropicana Gneiss|70182|5|Briefly described|p4|Archean|Archean|Tropicana Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen.|||||Interlayered granitic gneiss including tonalitic and dioritic compositions; mafic gneiss, including metagabbro and metamorphosed ultramafic rocks; garnet gneiss, and minor metachert and meta-iron formation.|
79293|Tropicana Gneiss|70254|4|Described|p355-357,374-376,379-381|Neoarchean|Archean|Geological province: Tropicana Domain, Yilgarn Craton, Albany-Fraser Orogen. Derived from the upthrusted eastern most margin of the underlying Yilgan Craton. Metamorphosed to mid-amphibolite to lower granulite facies in the period ca. 2638 to 2520 Ma, and exhumed (during Neoarchean Tropicana event?) to crustal levels equivalent to greenschist-facies conditions by the time of economic gold mineralisation ca. 2.5 Ga. Largely unaffected after economic mineralisation (except minor rutile peak ~<2.45 Ga) until Stage II Albany-Fraser Orogeny (Kirkland et al., 2011) but effects were minor and restricted to reactivation of older Neoarchean-Paleoproterozoic faults and shears. Detailed lithofacies descriptions of samples used for U-Pb, Re-Os and Ar geochronological analysis detailed on p361 Table 1. Weighted mean 207Pb/206Pb age of 2638+\-4 Ma indicates a minimum age for granitic magmatism. Pyrite Re-Os dating gives an age of 2505+\-50 Ma, broadly corresponding with late fluid-induced retrograde mineralisation.||||||
79293|Tropicana Gneiss|70256|5|Briefly described|p4-5|Archean|Archean|Amphibolite- to granulite-facies basement rocks of the Tropicana Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen. Gold-mineralisation at c.2500 Ma.|c.2640 Ma.|||Is overlain locally by Lindsay Hill Formation.|Amphibolite- to granulite-facies, locally migmatitic quartzofeldspathic gneiss, garnet-bearing gneiss, mafic to ultramafic gneiss, metachert, and meta-iron formation.|
79293|Tropicana Gneiss|70802|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Neoarchean|Geological province: Tropicana Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage II (1225-1140 Ma); Albany-Fraser Orogeny (1330-1140 Ma); Albany-Fraser Orogeny Stage I (1330-1260 Ma); Biranup Orogeny (1710-1620 Ma); Ngadju Event (1780-1760 Ma); Salmon Gums Event (1815-1800 Ma); Tropicana Event (2520-2505 Ma); Atlantis Event (2720-2550 Ma). See 500k_interpgeop14_lut.csv, 250k_pre_mesozoic_interpgeop_lut.csv.|2800-1600 Ma (inferred)||||Metamorphosed banded iron-formation, metagabbro and metaleucogabbro; may include Archean or Paleoproterozoic metagranite|
79293|Tropicana Gneiss|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Neoarchean|Geological province: Kepa Kurl Booya Province, Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage II (1225 - 1140 Ma); Albany-Fraser Orogeny (1330 - 1140 Ma); Albany-Fraser Orogeny Stage I (1330 - 1260 Ma); Biranup Orogeny (1710 - 1620 Ma); Ngadju Event (1780 - 1760 Ma); Salmon Gums Event (1815 - 1800 Ma); Tropicana Event (2520 - 2505 Ma); Atlantis Event (2720 - 2550 Ma). See 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|2800-1600 Ma (inferred)||||Interlayered granitic gneiss including tonalitic and dioritic compositions, mafic gneiss, garnet gneiss, and minor metachert and metamorphosed iron-formation; may include intrusions of Paleoproterozoic metagranite|
79293|Tropicana Gneiss|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Neoarchean|Tropicana Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen. This unit and two unnamed sub-units listed in the dataset. Various parts may include intrusions of Paleoproterozoic metagranite, Archean or Paleoproterozoic metagranite and unspecified metagranite.||||Remnants included in McKay Creek Metasyenogranite, Bobbie Point Metasyenogranite, Black Dragon Gneiss.|Interlayered granitic gneiss, mafic gneiss, garnet gneiss, minor metachert + meta-BIF. Meta-BIF, metagabbro + metaleucogabbro. Meta- gabbro + ultramafic rocks. Parts include or intruded by Archean, Paleoproterozoic or unspecified metagranite.|
79198|Truslove Suite|70182|5|Briefly described|p8-9, p34, p38, p45-47|Mesoproterozoic|Mesoproterozoic|New name, after Truslove historical township, N of Esperance. Stage II of the Albany-Fraser Orogeny. Trace-element unenriched granites. Geochemistry detailed; magmatic evolution discussed.||Esperance Supersuite.||||
79198|Truslove Suite|70802|4|Described|250k_pre_mesozoic_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage II (1225-1140 Ma); Albany-Fraser Orogeny (1330-1140 Ma). Sample GSWA 182459 (metatonalite) yielded a regression that intersects the concordia curve at 1156+\-5 Ma, interpreted as magmatic crystallisation age of the tonalite. Sample GSWA 194839 (metamonzogranite) yielded a concordia age of 1186+\-8 Ma, interpreted as magmatic crystallisation age of the monzogranite. Sample GSWA 194840 (metamonzogranite) yielded a weighted mean 207Pb*/206Pb* age of 1200+\-11 Ma, interpreted as magmatic crystallisation age of the monzogranite. See also geochron files.|1198+\-11 Ma; 1162+\-6 Ma|Unit of Esperance Supersuite.|||Dominantly monzogranite; undeformed to moderately deformed; may include magnetite-rich varieties|
79198|Truslove Suite|71270|4|Described|500k_interpgeop16_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage II (1225 - 1140 Ma); Albany-Fraser Orogeny (1330 - 1140 Ma). Sample 182459 (equigranular metatonalite) yielded a weighted mean 207Pb/206Pb age of 1156+\-5 Ma, interpreted to be the magmatic crystallisation age of the metatonalite.|1198+\-1 Ma; 1162+\-6 Ma|Unit of Esperance Supersuite.|||Dominantly monzogranite; undeformed to moderately deformed; may include magnetite-rich varieties|
79198|Truslove Suite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Albany-Fraser Orogen.|Max age 1198+/-11 Ma, min 1162+/-6 Ma.|Esperance Supersuite|||Dominantly monzogranite; undeformed to moderately deformed; may include magnetite-rich varieties.|
74831|Tuckanarra Suite|64891|4|Described|p34 Fig.1, p37 Fig. 2, p42, p52-53 Tb.1|Archean|Archean|Of Austin Downs Supersuite. Includes Pirgan, Karbar and Munarra Monzogranites. Ages range: 2686 to 2665Ma. Geol.prov: Murchison Domain. Consists of strongly foliated and locally magmatically layered granodiorite to monzogranitic rocks; metamorphosed.||||||07-FEB-11
74831|Tuckanarra Suite|66195|5|Briefly described|p599 Fig.2|Neoarchean||Granitic.||||||13-MAR-12
74831|Tuckanarra Suite|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Mapped as four separate but un-named units.|||||Quartz-feldspar porphyritic, fine-grained monzogranite; medium-grained, foliated leucocratic metamonzogranite; medium- to coarse-grained K-feldspar porphyritic metamonzogranite; foliated metagranodiorite, medium-grained to K-feldspar porphyritic.|
74831|Tuckanarra Suite|67129|6|Mentioned|p18 Fig.19, p19 Fig.20|Archean|Archean|Murchison Domain, Youanmi Terrane.|2690-2665 Ma||Karbar, Pirgan Monzogranites.||Granites.|07-SEP-17
74831|Tuckanarra Suite|68107|6|Mentioned|p619 Fig.8|||Western Youanmi Terrane.|||||Felsic magmatism.|
74831|Tuckanarra Suite|68108|5|Briefly described|p628, p649|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. Appears as Supersuite in p649.|ca. 2685-2665 Ma||||Granodiorite-monzogranites.|
74831|Tuckanarra Suite|68287|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Shown as younger than D1 deformation (2710-2690 Ma) and older than D2 deformation (2665 - 2640 Ma). K-feldspar megacrystic biotite metamonzogranite dated by Wang, Q. (1998 ?thesis) at c. 2668 Ma.|2690-2665 Ma||Includes Cundimurra Monzogranite.||Metamonzogranite to metagranodiorite; commonly foliated.|
74831|Tuckanarra Suite|68519|5|Briefly described|Map Legend|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|||||Metamonzogranite, medium to coarse grained, K-feldspar phenocrystic, foliated; biotite metamonzogranite, strongly foliated.|
74831|Tuckanarra Suite|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. Age: 2686 - 2665 Ma, from geochron file 178190.1.pdf, 178195.1.pdf.|||Includes 11 unnamed units and Cundimurra Monzogranite.|Intruded by Annean Supersuite granite.|Metamonzogranite to metagranodiorite; commonly foliated|
74831|Tuckanarra Suite|68698|5|Briefly described|p3-6, p8, p10-11, p14-20, p27-28|Neoarchean|Neoarchean|Intrudes the Meekatharra-Mount Magnet greenstone belt. Is locally cut by younger K-feldspar monzogranites. Affected by the late phase of shear-related deformation. A foliated granodiorite had a magmatic crystallisation age of 2675 +/- 3 Ma (Wingate et al., 2009). Geochemistry is discussed. REE plots. Lu-Hf isotope data and source regions discussed.|2686-2665 Ma.||||Strongly foliated and locally magmatically layered granodioritic to monzogranitic rocks.|
74831|Tuckanarra Suite|69014|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane.|2690-2665 Ma||Includes Cundimurra Monzogranite.|||
74831|Tuckanarra Suite|69583|4|Described|p49, p51-53, p99, p103, p105; Plate 2|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c.2690-2670 Ma.||Cundimurra, Munarra Monzogranites.|Is sheared against Windimurra Igneous Complex.|Metamonzogranite to metragranodiorite; commonly foliated.|
74831|Tuckanarra Suite|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean||||Cundimurra Monzogranite,  Munarra Monzogranite|||
74831|Tuckanarra Suite|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.|||Cundimurra, Munarra Monzogranites.|||
74831|Tuckanarra Suite|69626|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton|2690-2665 Ma||Cundimurra Monzogranite|||
74831|Tuckanarra Suite|69627|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton|c. 2680-c. 2676 Ma||Cundimurra Monzogranite|||
74831|Tuckanarra Suite|69744|6|Mentioned|p254||||c.2680-2660 Ma.|||||
74831|Tuckanarra Suite|70020|5|Briefly described|p118|Neoarchean|Neoarchean|Geological province: Yilgarn Craton.||||Overlain by Jungar Suite. Underlain by Big Bell Suite.||
74831|Tuckanarra Suite|70030|5|Briefly described|p191-192|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton.|2685-2665 Ma|||||
74831|Tuckanarra Suite|70139|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton. The four un-named facies are mapped separately.|2690-2665 Ma.||Munarra Monzogranite.||Biotite metamonzogranite, strongly foliated; quartz and feldspar porphyritic monzogranite, locally foliated; undeformed K-feldspar porphyritic monzogranite to syenogranite; undivided metamorphosed granite.|
74831|Tuckanarra Suite|70140|5|Briefly described|Map legend.|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. 6 facies are mapped separately.|2690-2665 Ma.||||Metamonzogranite to metagranodiorite; commonly foliated. Includes metagranites and metapegmatites.|
74831|Tuckanarra Suite|70153|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean||2690 - 2665 Ma (inferred).||||Metamonzogranite to metagranodiorite; commonly foliated.|
74831|Tuckanarra Suite|70156|4|Described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma).|2690-2665 Ma (inferred)||||Metamonzogranite to metagranodiorite; commonly foliated|
74831|Tuckanarra Suite|70418|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|2690-2665 Ma.||||Monzogranites; syenogranite, granite and metagranodiorite.|02-MAY-16
74831|Tuckanarra Suite|70419|5|Briefly described|p3, p10, p12-14, p17, p25, p26 Fig.10|Neoarchean|Neoarchean|Has a sheared contact with the Windimurra Igneous Complex and truncates many igneous layers. Density is 2.65 g/cm3.|c.2680 Ma.||||Syntectonic metamonzogranites.|
74831|Tuckanarra Suite|70420|6|Mentioned|p9 Fig.6|Archean|Archean|||||||
74831|Tuckanarra Suite|70770|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|2690-2657 Ma.||Cundimurra Monzogranite.||Metamonzogranites to metagranodiorite, commonly foliated.|
74831|Tuckanarra Suite|70794|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton. Also 2_5m_interpgeop15_lut.csv.|2690-2665 Ma inferred||||Metamonzogranite to metagranodiorite; commonly foliated.|
74831|Tuckanarra Suite|70796|4|Described|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton granite. See also 100k_geologyl_lut.csv, 100k_geologyp_lut.csv, 100k_geologysub_lut.csv,  100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 178190.1.pdf, 178195.1.pdf, 178199.1.pdf, 185997.1.pdf, 198212.1.pdf, 198213.1.pdf, 198220.1.pdf, Austin100_2442_stratig.pdf, Bungar100_2539_stratig.pdf, Challa100_2541_stratig.pdf, Coolamaninu100_2540_stratig.pdf, Cue100_2443_stratig.pdf, MountMagnet100_2441_stratig.pdf, Reedy100_2543_stratig.pdf, Windimurra100_2641_stratig.pdf, Wynyangoo100_2542_stratig.pdf, Youanmi100_2640_stratig.pdf.|2690 to 2665 Ma (inferred)||Includes the Munarra Monzogranite, Cundimurra Monzogranite, Pirgan Monzogranite and the Karbar Monzogranite.|Intrudes the Murchison Supergroup.|Finegrained granite, metamonzogranite to metagranodiorite; commonly foliated. Gneissose metagranodiorite, foliated metagranodiorite, strongly sheared metagranite, fine grained granite and quartz and feldspar porphyritic monzogranite.|
74831|Tuckanarra Suite|70826|6|Mentioned|p9|Neoarchean|Neoarchean||||||Granites.|
74831|Tuckanarra Suite|70830|5|Briefly described|p8-p10, p33, p40, p51, p58|Neoarchean|Neoarchean|Murchison Domain. |c. 2685-2665 Ma||||Granodiorite and monzogranite.|
74831|Tuckanarra Suite|71159|5|Briefly described|Map legend.||||||||Biotite metamonzogranite.|
74831|Tuckanarra Suite|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma). Zircon analysis from a monzogranite dyke intruding into the Crossroads Granodiorite yielded an interpteted magmatic crystallisation age of 2684+\-3 Ma (GSWA 155514). Sample GSWA 178195 (granitic gneiss) yielded a weighted mean 207Pb/206Pb date of 2675+\-5 Ma, interpreted to be the magmatic crystallisation age. Sample GSWA 178199 (foliated granodiorite) yielded a weighted mean 207Pb/206Pb date of 2675+\-3 Ma, interpreted to be the magmatic crystallisation age. Sample GSWA 198212 (porphyritic bt monzogranite) yielded a weighted mean 207Pb/206Pb date of 2681+\-5 Ma, interpreted to be the magmatic crystallisation age. Sample GSWA 198220 (bt monzogranite) yielded a weighted mean 207Pb/206Pb date of 2678+\-8 Ma, interpreted to be the magmatic crystallisation age. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv, 100k_geologysub_lut.csv.|2697+\-6, 2657+\-9 Ma (isotopic)||Includes Cundimurra Monzogranite, Karbar Monzogranite, Munarra Monzogranite, Pirgan Monzogranite.|Intrudes into Crossroads Granite. Intrudes Murchison Supergroup. Crosscut by bald Rock Supersuite.|Metamonzogranite: foliated, medium-grained to quartz to k-spar porphyritic, leucocratic, to metagranodiorite: gneissose, abundant rafts of amphibolitic metabasalt; fine-grained granite.|
74831|Tuckanarra Suite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|2690 (inferred); 2657+\-9 Ma||||Metamonzogranite to metagranodiorite; commonly foliated|
74831|Tuckanarra Suite|71271|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton.|||Munarra Monzogranite.||Metamonzogranites.|16-FEB-18
74831|Tuckanarra Suite|71809|5|Briefly described|map legend|Archean|Archean|Yilgarn Craton|||||Includes biotite metamonzogranite, strongly foliated; K-feldspar megacrystic biotite metamonzogranite,  strongly foliated; quartz and feldspar-phyric fine-grained monzogranite, locally foliated.|
74831|Tuckanarra Suite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||Max age ~2690 Ma, min age 2657+/-9 Ma.||Includes Munarra Monzogranite, Cundimurra Monzogranite and an innamed unit.||Metamonzogranite to metagranodiorite; commonly foliated. K-feldspar megacrystic biotite metamonzogranite; strongly foliated.|
74831|Tuckanarra Suite|72389|5|Briefly described|Map Legend|Archean|Archean|Yilgarn Craton. Gabanintha 1:100k map sheet 2644. Includes  a foliated metamonzogranite and an unnamed biotite metamonzogranite member dated at c. 2681 Ma.|2697-2657 Ma||||Metamonzogranite to metagranodioriote; commonly foliated.|28-AUG-20
74831|Tuckanarra Suite|73410|6|Mentioned|p2|||Youanmi Terrane.|2690-2665 Ma.|||||
74831|Tuckanarra Suite|73596|6|Mentioned|p1168|Neoarchean|Neoarchean|Yilgarn Craton.|2690-2665 Ma.|||||
24538|Tuckfield Member|7433|5|Briefly described|pp34-36.  |||In north and northeast, silty units often carbonaceous and plant-bearing.||Middle unit in Poole Sandstone.||Overlies Nura Nura Member and, locally, Carolyn Formation. Is overlain by Christmas Creek Member.|Fine-grained quartzose sandstone; minor siltstone; intraformational mud-clast conglomerates locally. Planar laminated throughout, with muscovite flakes on bedding surfaces. Ripple-marks and cross-stratification common.|
24538|Tuckfield Member|22718|6|Mentioned|P5|||||||||
24538|Tuckfield Member|22741|5|Briefly described|P27, P28, Table3 P13|Artinskian|Artinskian|||||||
24538|Tuckfield Member|22765|6|Mentioned|P10|||||||||
24538|Tuckfield Member|22767|5|Briefly described|Table3 P16, P21||Early Permian|||||||
24538|Tuckfield Member|22776|4|Described|Table.3|Early Permian|Early Permian|Parent: Poole Sandstone||||||
24538|Tuckfield Member|24466|4|Described|p367-368|Early Permian|Early Permian|Of the Poole Sandstone.  Overlies the Nura Nura Member; conformably overlain by the Christmas Creek Member.||||||
24538|Tuckfield Member|36224|5|Briefly described|Map legend|Early Permian|Early Permian|Of the Poole Sandstone.  Sandstone, minor mudstone; plant fossils.||||||01-FEB-05
24538|Tuckfield Member|36225|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
24538|Tuckfield Member|36634|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
24538|Tuckfield Member|42613|2|Defined|P 14, 16|Artinskian|Artinskian|of Poole Sandstone||||||
24538|Tuckfield Member|45158|4|Described|p20|||||||||
24538|Tuckfield Member|66949|4|Described|p20, p23, p57 Appx.3|Artinskian|Artinskian|Name proposed by Crowe and Towner (1976). Outcropping type section detailed. Up to 160m thick; deltaic to fluvial deposits. Similar to overlying Christmas Creek Member.||Unit in Poole Sandstone.||Overlies Nura Nura Member; is overlain by Christmas Creek Member.|Coarsening-upward sandstone, minor siltstone.|02-NOV-15
24538|Tuckfield Member|70774|5|Briefly described|p7|||Previously the middle sub-division of the Poole Sandstone before being formally abandoned as unecessary by Mory (2010).||||||
27594|Tulki Limestone|12491|6|Mentioned|p454 Fig.7|Miocene|Oligocene|Presented in figure as Trealla/ Tulki/ Mandu. Tertiary marls.||||||06-NOV-14
27594|Tulki Limestone|23726|5|Briefly described|p90|Miocene|Oligocene|Overlying unit Muiron Member. Underlying unit Pilgramunna Formation. Geological Province: Carnarvon Basin.||||||
27594|Tulki Limestone|23815|4|Described|p302, p313 Fig.40|Miocene|Miocene|Age: Middle Miocene. Geological Province: Carnarvon Basin. Overlying unit: Trealla Limestone (disconformable). Underlying unit: Mandu Calcarenite (conformable). Max. thickness: 66 m. Fossiliferous.||||||18-APR-05
27594|Tulki Limestone|24059|5|Briefly described|p133|Oligocene|Oligocene|Of Cape Range Group. Geological Province: Barrow Sub-basin.||||||
27594|Tulki Limestone|24084|5|Briefly described|p146 Fig.2|Miocene|Miocene|Geological Province: North Carnarvon Basin.||||||16-MAR-05
27594|Tulki Limestone|24094|5|Briefly described|p269, p288|Early Miocene|Early Miocene|Overlies Mandu Calcarenite. Geological Province: Carnarvon Basin||||||16-MAR-05
27594|Tulki Limestone|24351|5|Briefly described|Plate 4 (in pocket)|Middle Miocene|Early Miocene|Geological Province: Exmouth Sub-basin (onshore).||||||13-DEC-07
27594|Tulki Limestone|30122|4|Described|p47|||See also P48-49||||||
27594|Tulki Limestone|30821|5|Briefly described|p59|||Stratigraphic sequence on table.||||||
27594|Tulki Limestone|31623|6|Mentioned|p120|||Caves. Refers Cook (1962)||||||
27594|Tulki Limestone|32648|6|Mentioned|p32|||in Cape Range Gp.||||||
27594|Tulki Limestone|32750|6|Mentioned|p311|||Refers Condon (1968)||||||
27594|Tulki Limestone|33593|6|Mentioned|p107|||Refs Condon and others 1953,2nd Ed 1955||||||
27594|Tulki Limestone|35105|6|Mentioned|Fig.5|||||||||
27594|Tulki Limestone|35282|6|Mentioned|p27|||||||||
27594|Tulki Limestone|36257|6|Mentioned|Table 2.1|||||||||
27594|Tulki Limestone|36747|6|Mentioned|p104|||||||||
27594|Tulki Limestone|36890|3|Fully described|p302|||||||||
27594|Tulki Limestone|37016|6|Mentioned|Map legend|middle Miocene|middle Miocene|||||||
27594|Tulki Limestone|39427|4|Described|Table 1|||||||||
27594|Tulki Limestone|40617|6|Mentioned|p18|||||||||
27594|Tulki Limestone|41271|3|Fully described|p179|||||||||
27594|Tulki Limestone|41438|6|Mentioned|Fig.23|||||||||
27594|Tulki Limestone|41732|6|Mentioned|Fig.3|||||||||
27594|Tulki Limestone|42116|5|Briefly described|p70|||||||||
27594|Tulki Limestone|42734|5|Briefly described|map legend|Tertiary||||||||
27594|Tulki Limestone|44959|3|Fully described|p.23|||||||||
27594|Tulki Limestone|45015|5|Briefly described|map legend|Tertiary|Tertiary|Of the Cape Range Group. Age is Late Tertiary.||||||01-JUN-06
27594|Tulki Limestone|45168|6|Mentioned|p6|||||||||
27594|Tulki Limestone|46805|6|Mentioned|p171|||||||||
27594|Tulki Limestone|46983|6|Mentioned|Fig.2|Tertiary|Tertiary|See also informal references on p107, 191.||Of Cape Range Group.||||21-JAN-22
27594|Tulki Limestone|48831|14|Not recorded|p.14,26,30,31|||||||||
27594|Tulki Limestone|61155|5|Briefly described|P15|Early Miocene|Early Miocene|Of the Cape Range Group. Age: ~23-19.5Ma. Thickness: 100m.  Geological Province: Carnarvon Basin /onshore.||||||20-DEC-06
27594|Tulki Limestone|61958|5|Briefly described|Map sheet 1|Neogene|Neogene|Of the Cape Range Group.||||||
27594|Tulki Limestone|62837|5|Briefly described|Stratigraphic columns|Middle Miocene|Middle Miocene|Age: >15Ma. Geological Province: Exmouth and Barrow Sub-basins.||||||07-NOV-06
27594|Tulki Limestone|66125|6|Mentioned|p133 Fig.4|||Ningaloo Reef. Tertiary limestone.||||Is overlain by Pilgramunna Formation and Bundera Calcarenite.||
27594|Tulki Limestone|67200|5|Briefly described|p8 fig 6, |Miocene|Oligocene|||||Unconformably overlain by Pindilya Formation, Lamont Sandstone, Trealla Limestone|Crudely and planar cross bedded limestone.|
27594|Tulki Limestone|68811|6|Mentioned|p108 fig 62|||||||||
27594|Tulki Limestone|70066|5|Briefly described|Regional: Fig.6|Burdigalian|Aquitanian|Exmouth Sub-basin, Northern Carnarvon Basin.||||Overlies Bullara Limestone. Is overlain by Trealla Limestone.||
27594|Tulki Limestone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||packstone|
31888|Tumagee Granite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.||||||07-NOV-08
31888|Tumagee Granite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1850Ma. Geological province: Kimberley Province (East).||||||07-FEB-11
31888|Tumagee Granite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
31888|Tumagee Granite|43854|5|Briefly described|Map Legend||Proterozoic|Of Paperbark supersuite.||||||
31888|Tumagee Granite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31888|Tumagee Granite|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite.||||||07-NOV-08
31888|Tumagee Granite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Paperbark Supersuite|||Medium-grained, equigranular or weakly porphyritic biotite monzogranite and granodiorite; minor tonalite.|04-AUG-15
31888|Tumagee Granite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Paperbark Supersuite|||Medium grained, equigranular or weakly porphyritic biotite monzogranite and granodiorite; minor tonalite.|
31888|Tumagee Granite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone.|1864-1852 Ma (Inferred)|Unit of Paperbark Supersuite.|||Medium-grained, equigranular or weakly porphyritic biotite monzogranite and granodiorite; minor tonalite|
31888|Tumagee Granite|70154|6|Mentioned|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1852-1864 Ma|Paperbark Supersuite||||
31888|Tumagee Granite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (183 -1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1864-1852 Ma (inferred)|Unit of Paperbark Supersuite.|||Medium-grained, equigranular or weakly porphyritic biotite monzogranite and granodiorite; minor tonalite|
31888|Tumagee Granite|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen, North Australian Craton.||Paperbark Supersuite.|||Medium-grained, equigranular or weakly porphyritic biotite monzogranite and granodiorite; minor tonalite.|
31888|Tumagee Granite|72437|5|Briefly described|p79-80, p82, p85|||Lamboo Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Hornblende-biotite granodiorite, quartz-phyric granodiorite and fine-grained biotite monzogranite.|
33832|Turee Creek Supersequence|22546|4|Described|370||Archean|Geol province Turee Creek Basin. Max thickness 3100 m. Max age 2405 Ma. Overlies Woongara Sequence. Overlain by Wyloo Supersequence.||||||07-NOV-08
33832|Turee Creek Supersequence|22682|5|Briefly described|Fig20,p29|Siderian|Siderian|2452-2408 Ma.||||||03-MAR-10
33832|Turee Creek Supersequence|71112|6|Mentioned|p69,80|Archean|Archean|Geological province: Pilbara Craton. Encompasses the entire Turee Creek Group, and Boolgeeda Iron Formation.||||||
81575|Turkey Creek Gabbro|71873|5|Briefly described|p426-427,431-440,442,444|Orosirian|Orosirian|Geological province: Lamboo Province. A dyke-like body that cross-cuts the Sally Malay Suite intrusions. U-Pb detrital zircon magmatic age include 1843+\-5 and 1848+\-5 Ma (tentative magmatic age). Metamorphic ages from disturbed, recrystallized or new-growth zircon rims include 1846+\-9 Ma, interpreted to represent a younger phase of a 1845 Ma event, where HT metamorphism and mafic-ultramafic magmatism were coeval.||Not a unit of Sally Malay Suite.|||Hornblende-bearing non-cumulate gabbronorites.|03-SEP-19
78347|Turret Dolerite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2691 Ma (inferred).||||Dolerite, medium grained; minor gabbro; metamorphosed. Pyroxenite, medium grained, metamorphosed.|
78347|Turret Dolerite|70326|3|Fully described|p334,336,338-9,341,346,350-7,360,362-3|Neoarchean|Neoarchean|Geological province: Agnew region, Ora Banda Domain, Kalgoorlie Terrane, Yilgarn Craton. [Misspelt as Turrett Dolerite on p334,350-351,355,357]. Differentiated high-Th mafic sill with extreme LREE enrichment and represents the youngest preserved major magmatic event of the section. Total thickness: 300 m. Agnew Anticline: observed in several drillholes on the eastern limb. Not found on the western limb. In contact with Vivien Formation via sheared unconformity. Evidence of crustal contamination e.g. negative Nb and T ianomalies; [La/Sm]PM> 1; Pearce, 2008; van Hunen and Moyen, 2012). TIMS U-Pb zircon age of 2690.7+\-1.2 Ma (interpreted crystallisation age).|2690.7+\-1.2 Ma|||Overlain by Mosquito Well Conglomerate. Underlain by White Hope Basalt. Correlable to Ora Banda and Grrenfields sillls, and Defiance and Williamstown dolerites.|Coarse-grained basic-ultrabasic LFA (dolerite, gabbro, cumulate ultrabasic LF and rare basalt and granophyre LF). Differentiated sill.|
78347|Turret Dolerite|71212|5|Briefly described|intro p2, intro p3|||Yilgarn Craton. Equivalent to the informal Vivien Gabbro.||Two Sisters Subgroup||||
78347|Turret Dolerite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2691 Ma (inferred)||||Dolerite, medium grained; minor gabbro; metamorphosed; pyroxenite, medium-grained; metamorphosed.|
78347|Turret Dolerite|73151|5|Briefly described|p3, p5, p10, p12-13|Neoarchean|Neoarchean|Yilgarn Craton. Kalgoorlie Terrane, Agnew Greenstone Belt.||Kalgoorlie Group||Overlies the White Hope Basalt, faulted beneath the Vivean Formation.|Dolerite sill, ultrabasic cumulate at base.|
78347|Turret Dolerite|73238|6|Mentioned|p13 Fig.10|||Agnew district, Mount White Basin, Eastern Goldfields Terrane. Appears in Fig.10 as Vivien (Turret) Dolerite.||||||
78347|Turret Dolerite|73596|6|Mentioned|p1152, 1156-1158, 1160|Neoarchean|Neoarchean|Lawlers-Mount White Domain, Agnew-Wiluna Greenstone Belt.|2691 +/- 1 Ma.|||Emplaced between Two Sisters Subgroup and overlying Vivien Formation. Is overlain unconformably by Scotty Creek Formation.|Differentiated basalt-dolerite-gabbro-granophyre plutonic complex.|
79568|Twin Hills Monzogranite|71270|4|Described|100k_interpgeop_lut.csv|Mesoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2803+\-3 Ma ||||Metamonzogranite; foliated to gneissic; intruded by leucocratic monzogranite and late pegmatite dykes|
68502|Twin Table Monzogranite|63441|2|Defined|p10 Tb. 2, p36|Archean|Archean|Of the Railway Supersuite. Intrudes Nallana Formation. Age: 3114+/-5Ma. Geological province: Pilbara Craton. Outcrops as stocks of foliated, medium-grained monzogranite and granodiorite within the Nallana Fm (Whundo Group).||||||07-FEB-11
68502|Twin Table Monzogranite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Railway Supersuite.  Age range: 3123-3114Ma. Geological province: Sholl Terrane, West Pilbara Superterrane. Monogranite and alkali feldspar granite; metamorphosed.||||||07-NOV-08
68502|Twin Table Monzogranite|64580|4|Described|map legend|Archean|Archean|Of Railway Supersuite. Monzogranite and alkali feldspar granite; metamorphosed.||||||15-DEC-08
68502|Twin Table Monzogranite|67201|5|Briefly described|p16-17 Fig.9|Archean|Archean|In northwestern Pilbara Craton, Sholl Terrane, West Pilbara Superterrane.||Railway Supersuite|||Monzogranite and alkali-feldspar granite; metamorphosed.|
68502|Twin Table Monzogranite|69185|4|Described|500k_geologyp08_lut.csv|Archean|Archean|Geological Province: Pilbara Craton.||Unit of Railway Supersuite.|||Gneissic metamonzogranite; locally migmatitic, and veined by younger granitic rocks; locally contains large mafic and ultramafic xenoliths|
68502|Twin Table Monzogranite|70775|5|Briefly described|p15|||Sholl Terrane, Pilbara Craton.||Railway Supersuite|||Monzogranite and alkali-feldspar granite; metamorphosed.|
68502|Twin Table Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, alkali feldspar granite|
68502|Twin Table Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||3114+/-5 Ma.|Railway Supersuite|||Monzogranite and alkali-feldspar granite; metamorphosed.|
73785|Two Bobs pegmatite|50542|6|Mentioned|p95, p95 Table 27.|||Informal name. A series of parallel and interconnecting pegmatite bodies. Maximum Thickness: 300m. Hosts the Two Bobs prospect. Lithology: placer, granitic rare-metal pegmatite.||||||07-FEB-11
77949|Two Sisters Subgroup|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2720 - 2680 Ma (inferred).|Kalgoorlie Group|Includes White Hope, Redeemer, Burrell Well Basalts; Agnew Komatiite.|||
77949|Two Sisters Subgroup|71212|5|Briefly described|intro p2, intro p3|||Yilgarn Craton. |||Includes the White Hope Basalt, Redeemer Basalt, Burrell Well Basalt, the Turret Dolerite and the Agnew Komatiite.|||
77949|Two Sisters Subgroup|71270|5|Briefly described|100k_interpgeop_lut.csv|||Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. ||Unit of Kalgoorlie Group.|Includes Agnew Komatiite, Burrell Well Basalt, Never Can Tell Basalt, Redeemer Basalt, White Hope Basalt.|||
77949|Two Sisters Subgroup|72095|6|Mentioned|p5 Fig 3|Neoarchean|Neoarchean|Eastern Goldfields, Yilgarn Craton.||Unit of Kalgoorlie Group.||||
77949|Two Sisters Subgroup|73596|6|Mentioned|p1153, 1155-1158, 1160, 1162-1163|Neoarchean|Neoarchean|Agnew-Wiluna Greenstone Belt.|c.2720-2690 Ma.||Never Can Tell, Burrell Well, Redeemer, White Hope Basalts; Agnew Komatiite.|Overlies Cosmos Volcanic Complex. Is overlain by Vivien Formation. Is faulted against Scotty Creek Formation.||
31861|Tyama Granite|24197|5|Briefly described|p102 Tb. 14.1|Neoproterozoic|Neoproterozoic|Of O'Callaghans Supersuite. Geological province: Paterson Orogen.||||||
31861|Tyama Granite|50436|5|Briefly described|p1.3, Table 1.1|Neoproterozoic|Neoproterozoic|Geological Province: Paterson Orogen. Of the O'Callaghans Supersuite.||||||
24053|Uaroo Group|23311|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
24053|Uaroo Group|24183|6|Mentioned|p12|||Correlated with the Cheyne Springs Formation.||||||
24053|Uaroo Group|36902|6|Mentioned|p17|||||||||
24053|Uaroo Group|37016|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24053|Uaroo Group|37299|6|Mentioned|p88|||||||||
24053|Uaroo Group|37422|6|Mentioned|p8|||||||||
24053|Uaroo Group|38482|4|Described|p17|||||||||
24053|Uaroo Group|38988|6|Mentioned|p14|||||||||
24053|Uaroo Group|39427|2|Defined|p4|Precambrian|Precambrian|||||||
24053|Uaroo Group|40088|6|Mentioned|p227|||||||||
24053|Uaroo Group|40089|6|Mentioned|p12|||||||||
24053|Uaroo Group|40900|4|Described|p32|||||||||
24053|Uaroo Group|40935|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24053|Uaroo Group|40937|3|Fully described|p5|||||||||
24053|Uaroo Group|41271|6|Mentioned|p9|||||||||
24053|Uaroo Group|44142|5|Briefly described|p317, p326 Tb.4-5||||||Includes Tinkers and Mulyu Dolomites, Mandorah Shale and Rouse Creek Arenite.|Unconformably overlies Gascoyne Complex. Basal part is correlated with Cheyne Springs Formation.||13-MAR-18
24053|Uaroo Group|64580|4|Described|map legend|Mesoproterozoic|Paleoproterozoic|Of Bangemall Supergroup. Sandstone, siltstone, mudstone, dolostone, and chert; minor conglomerate.||||||09-DEC-08
24053|Uaroo Group|69166|4|Described|500k_geologyp08_lut.csv|Mesoproterozoic|Paleoproterozoic|||Bangemall Supergroup|||Undivided; sandstone, siltstone, mudstone, dolostone, and chert; minor conglomerate.|
24053|Uaroo Group|69185|5|Briefly described|500k_geologyp08_lut.csv|Mesoproterozoic|Paleoproterozoic|||Unit of Bangemall Supergroup.|||Undivided; sandstone, siltstone, mudstone, dolostone, and chert; minor conglomerate|
24053|Uaroo Group|70795|4|Described|500k_interpgeop14_lut.csv|Mesoproterozoic|Paleoproterozoic||1620-1500 Ma||||Sandstone, siltstone, mudstone, dolostone and chert with minor conglomerate.|
24053|Uaroo Group|70826|6|Mentioned|p5 tbl 2|||Edmund Basin.||Bangemall Supergroup||||
24053|Uaroo Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||crystalline dolostone/dolomite, sandstone|
24053|Uaroo Group|72259|6|Mentioned|p3|Calymmian|Statherian|||||||
34584|Ularring Monzogranite|22841|5|Briefly described|Map legend||Archean|Variation on Ularring Granite||||||07-NOV-08
34584|Ularring Monzogranite|22890|6|Mentioned|P13|||||||||
34584|Ularring Monzogranite|23531|5|Briefly described|p21.|||||||||
34584|Ularring Monzogranite|24167|5|Briefly described|p38|Archean|Archean|Age: c2632Ma.||||||07-NOV-08
34584|Ularring Monzogranite|24494|5|Briefly described|p12|Archean|Archean|Age: 2632 +/- 4 Ma (U-Pb; Nelson, 2000)||||||07-NOV-08
34584|Ularring Monzogranite|50075|5|Briefly described|p18|Archean|Archean|Age: 2632 +/- 4 Ma (U-Pb) Nelson, 1996. Geological Province: Yilgarn Craton.||||||07-NOV-08
34584|Ularring Monzogranite|60076|6|Mentioned|p46 App. 1|||[Agmul]   Even-grained monzogranite.||||||
34584|Ularring Monzogranite|65264|5|Briefly described|p48 Appdx. 1|Archean|Archean|Even-grained monzogranite.||||||07-FEB-11
34584|Ularring Monzogranite|68289|5|Briefly described|p20|||Ovoid pluton within the southern part of the Mount Ida greenstone belt.|||||Fine- to coarse-grained, weakly seriate, biotite monzogranite with minor opaque oxides, muscovite and rare apatite. Secondary minerals include epidote, chlorite and rare fluorite.|
34584|Ularring Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Even-grained monzogranite.|07-AUG-15
34584|Ularring Monzogranite|69631|5|Briefly described|p30, p34|Neoarchean|Neoarchean|Wyche (2004). An ovoid pluton within the southern part of the Mount Ida greenstone belt.|2632 +/- 4 Ma (SHRIMP U-Pb zircon; Nelson, 2000).||||Fine- to coarse-grained, weakly seriate, biotite monzogranite containing minor opaque oxides, muscovite, are rare apatite. Weakly recrystallised, but mainly undeformed.|
34584|Ularring Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|See also 500k_interpgeop14_lut.csv.|2632 +/- 4 Ma (isotopic).||||Even-grained monzogranite.|
34584|Ularring Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
34584|Ularring Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv.|2632+\-4 Ma||||Even-grained monzogranite|
34584|Ularring Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||2632+/-4 Ma||||Even-grained monzogranite.|
76098|Umutju Granite|66284|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province.||Unit in Pitjantjatjara Supersuite.|||Medium- to coarse-grained hornblende-pyroxene-(garnet) granite; metamorphosed.|
76098|Umutju Granite|67128|5|Briefly described|p30|||Scrimgeour et al. (1999). Musgrave Orogeny: part of the basement to the Giles Event.|c.1140 Ma.|Pitjantjatjara Supersuite.||||
76098|Umutju Granite|67375|5|Briefly described|p178.|Mesoproterozoic|Mesoproterozoic|This is the main  basement lithology found throughout, and to the north of, the Mann Ranges in the Northern Territory; is inferred to dominate the bedrock geology beneath regolith cover in the northeastern part of the Walpa Pulka Zone (northern part of BATES).|1175 +/- 10 - 1145 +/- 6 Ma (Edgoose et al. 2004).|Unit in Umutju Suite.|||Medium- to coarse-grained hornblende-pyroxene granite metamorphosed at granulite facies; plagioclase or K-feldspar phenocrysts.|
76098|Umutju Granite|69153|5|Briefly described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Paterson Orogen, Musgrave Province. Umutju Granite is in sub-part Pitjantjatjara Supersuite 2.||Pitjantjatjara Supersuite|||Medium- to coarse-grained hornblende-pyroxene(-garnet) metagranite|
76098|Umutju Granite|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|Musgrave Province/(Complex?)|1148 Ma - 1175 Ma (Isotopic)|Pitjantjatjara Supersuite|||Medium- to coarse-grained hornblende--pyroxene(--garnet) metagranite|
33650|Umutju Granite Suite|24301|6|Mentioned|p37 Appendix 1|||||||||
33650|Umutju Granite Suite|60572|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the Mantapyika and Puka Granites.  Age: ~1180-1120Ma.  Geological Province: Musgrave Block.||||||
33650|Umutju Granite Suite|60683|2|Defined|p55 Appendix, p14|Mesoproterozoic|Mesoproterozoic|Includes Mantapayika, Puka and Walytjatjata Granites and unnamed charnockite and clinopyroxene granite.  Synonymous with part of Musgrave-Mann Metamorphics, Olia Gneiss and unnamed metamorphosed granites of Forman (1966a, 1972). See also p10 Tb.1, p42-43.||||||
33650|Umutju Granite Suite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the Walytjatjata, Puka and Mantapayika Granites. Age: ~1180-1120Ma. Geological Province: Musgrave Block.||||||19-OCT-05
33650|Umutju Granite Suite|69091|6|Mentioned|p103 Fig.5.6|||||||||
33650|Umutju Granite Suite|70793|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma); Musgrave Orogeny (1220-1150 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 500k_interpgeop_lut.csv.|1175+\-10 Ma; 1148+\-6 Ma|Unit of Pitjantjatjara Supersuite.|||Medium- to coarse-grained hornblende-pyroxene(-garnet) metagranite|
33650|Umutju Granite Suite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||charnockite, migmatite, granite|
33650|Umutju Granite Suite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|1175+\-10 Ma; 1148+\-6 Ma|Unit of Pitjantjatjara Suite.|||Medium- to coarse-grained hornblende--pyroxene(--garnet) metagranite|
33650|Umutju Granite Suite|71592|5|Briefly described|Appendix A.|||Musgrave Province. Age determination by zircon Pb-Pb evaporation.|1172+/-6 Ma (crystallisation).||||Granite.|
33650|Umutju Granite Suite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Musgrave Province, Paterson Orogen.|Max age 1175+/-10 Ma, Min 1148+/-6 Ma.|Pitjantjatjara Supersuite|||Medium- to coarse-grained hornblende-pyroxene(-garnet) metagranite.|
79175|Undawidgi Supersuite|70831|5|Briefly described|p25-p26|Calymmian|Calymmian|Coompana Province. Misspelt as the Undawidji Supersuite on p25.|c. 1505-1487 Ma|||||
79175|Undawidgi Supersuite|71143|5|Briefly described|p427,429,431-432,434,434,440|Calymmian|Calymmian|Geological province: Coompana Province. Alkali-calcic to alkalic, high-K to shoshonitic suite. Transitional A-type felsic rocks with a crustal source component that was primitive and likely hydrated and oxidised  (contains juvenile isotope values consistent with extensional processes involving asthenospheric input). May reflect recycling of c. 1600 Ma arc crust of the Toolgana Supersuite, with additional but variable juvenile mantle input (Smithies et al., 2015b).|c. 1490 Ma|||||
79175|Undawidgi Supersuite|71165|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Western Coompana Province.|c.1490 Ma.|||Is intruded by Moodini Supersuite.|Foliated metagranite and felsic metavolcanic rocks.|
79175|Undawidgi Supersuite|71891|5|Briefly described|p7|||Coompana Province.|c. 1490 Ma||||Metagranitic and possibly bimodal metavolcanic rocks. Variably foliated metatonalites and metamonzogranites, metamonzodiorites and variably sheared/mylonitic felsic and mafic schists.|
79175|Undawidgi Supersuite|72242|5|Briefly described|p27,31|Calymmian|Calymmian|Geological province: Coompana Province. A-type magmatism, post-dating Kararan Orogeny. |c. 1505-1487 Ma||||Granitic gneiss.|
79175|Undawidgi Supersuite|72344|5|Briefly described|p3, p5-p7, p9, p61, p63, p71|Calymmian|Calymmian|Coompana Province. Rift related and interpreted to include recycled Toolgana Supersuite material. Similar in age to the granodiorite gneiss from Mallabie 1 drillhole. Ages are derived from Fraser and Neumann, 2016 and Wingate et al, 2015a. See also p143.|1487-1526 Ma (SHRIMP U-Pb)||Includes the Gilgerabbie Suite and Bunburra Suite.||Metagranitic and possible bimodal metavolcanic rocks including variably foliated metatonalites and metamonzogranites, which are locally gneissic and migmatitc, metamonzodiorites and variably sheared/mylonitic felsic and mafic schists.|04-SEP-19
79175|Undawidgi Supersuite|72465|5|Briefly described|p4, 10|||Coompana Province. Extension and rift-related; derived by melting of lower mafic crust and a mantle component. Underwent metamorphism 1174 +/- 12 Ma.|1505 +/- 7 Ma to 1487 +/- 9 Ma.||||Variably foliated metatonalites and metamonzogranites, locally gneissic and migmatitic; metamonzodiorites; and variably sheared/mylonitic felsic and mafic schists (of monzogranitic or volcanic protolith).|
79175|Undawidgi Supersuite|72466|5|Briefly described|p4, 10|||Basement to Coompana Province. Extension and rift-related; rocks derived from melting of lower mafic crust, recycled Toolgana Supersuite material, and introduction of a mantle component. Metamorphosed at 1174 +/- 12 Ma.|1613/- 13 Ma to 1591 +/- 11 Ma.||||Variably foliated metatonalites and metamonzogranites, locally gneissic and migmatitic; metamonzodiorites; and variably sheared/mylonitic felsic and mafic schists (the former with ?monzogranitic or volcanic protolith).|
79175|Undawidgi Supersuite|72467|5|Briefly described|p4, 10|||Coompana Province. Extension and rift-related; derived by melting of lower mafic crust and a mantle component. Underwent metamorphism 1174 +/- 12 Ma.|1505 +/- 7 Ma to 1487 +/- 9 Ma.||||Variably foliated metatonalites and metamonzogranites, locally gneissic and migmatitic; metamonzodiorites; and variably sheared/mylonitic felsic and mafic schists (of monzogranitic or volcanic protolith).|
79175|Undawidgi Supersuite|72468|5|Briefly described|p4, p10|Calymmian|Calymmian|Coompana Province. Derived by melting of lower mafic crust and the introduction of a mantle component. Also interpreted to include recycled Toolgana Supersuite material. Magmatic ages include 1505 +/- 7 Ma, 1499 +/- 9 Ma, 1488 +/- 4 Ma, and 1487 +/- 9 Ma. Metamorphic age of 1174 +/- 12 Ma.|c. 1500-1490 Ma||||Metagranitic and possible bimodal metavolcanic rocks including variably foliated metatonalites and metamonzogranites, which are locally gneissic and migmatitic; metamonzodiorites; and variably sheared/mylonitic felsic and mafic schists.|
79175|Undawidgi Supersuite|72469|5|Briefly described|p4, p10|Calymmian|Calymmian|Coompana Province. Derived by melting of lower mafic crust and the introduction of a mantle component. Also interpreted to include recycled Toolgana Supersuite material. Magmatic ages include 1505 +/- 7 Ma, 1499 +/- 9 Ma, 1488 +/- 4 Ma, and 1487 +/- 9 Ma. Metamorphic age of 1174 +/- 12 Ma.|c. 1500-1490 Ma||||Metagranitic and possible bimodal metavolcanic rocks including variably foliated metatonalites and metamonzogranites, which are locally gneissic and migmatitic; metamonzodiorites; and variably sheared/mylonitic felsic and mafic schists.|
79175|Undawidgi Supersuite|72470|5|Briefly described|p4, p10|Calymmian|Calymmian|Coompana Province. Derived by melting of lower mafic crust and the introduction of a mantle component. Also interpreted to include recycled Toolgana Supersuite material. Magmatic ages include 1505 +/- 7 Ma, 1499 +/- 9 Ma, 1488 +/- 4 Ma, and 1487 +/- 9 Ma. Metamorphic age of 1174 +/- 12 Ma.|c. 1500-1490 Ma||||Metagranitic and possible bimodal metavolcanic rocks including variably foliated metatonalites and metamonzogranites, which are locally gneissic and migmatitic; metamonzodiorites; and variably sheared/mylonitic felsic and mafic schists.|
79175|Undawidgi Supersuite|72471|5|Briefly described|p4, p10|Calymmian|Calymmian|Coompana Province. Derived by melting of lower mafic crust and the introduction of a mantle component. Also interpreted to include recycled Toolgana Supersuite material. Magmatic ages include 1505 +/- 7 Ma, 1499 +/- 9 Ma, 1488 +/- 4 Ma, and 1487 +/- 9 Ma. Metamorphic age of 1174 +/- 12 Ma.|c. 1500-1490 Ma||||Metagranitic and possible bimodal metavolcanic rocks including variably foliated metatonalites and metamonzogranites, which are locally gneissic and migmatitic; metamonzodiorites; and variably sheared/mylonitic felsic and mafic schists.|
79175|Undawidgi Supersuite|72472|5|Briefly described|p4, p10|Calymmian|Calymmian|Coompana Province. Derived by melting of lower mafic crust and the introduction of a mantle component. Also interpreted to include recycled Toolgana Supersuite material. Magmatic ages include 1505 +/- 7 Ma, 1499 +/- 9 Ma, 1488 +/- 4 Ma, and 1487 +/- 9 Ma. Metamorphic age of 1174 +/- 12 Ma.|c. 1500-1490 Ma||||Metagranitic and possible bimodal metavolcanic rocks including variably foliated metatonalites and metamonzogranites, which are locally gneissic and migmatitic; metamonzodiorites; and variably sheared/mylonitic felsic and mafic schists.|
79175|Undawidgi Supersuite|72934|5|Briefly described|p2, p4, p12, App.A|Calymmian|Calymmian|Geochemically and temporally similar to the Gilgerabbie Suite. Associated with, but slightly postdates Bunburra Suite magmatism. Possibly reflects recycling of c. 1600 Ma arc crust of the Toolgana Supersuite with additional mantle input.|c. 1490 Ma||||Metamorphosed syenogranite, monzogranite, tonalite, monzodiorite, syenite, and felsic volcanic rocks.|
79175|Undawidgi Supersuite|72947|5|Briefly described|p4, p7-9, p11, p13|Calymmian|Calymmian|Coompana Province. Derived by melting of lower mafic crust with mantle input during lithospheric extension.|c. 1500 Ma / 1505 - 1487 Ma||Gilgerabbie Suite||A-type rocks.|
79175|Undawidgi Supersuite|73084|4|Described|p: 12, 15, ~38-47, 69-70, 72-73...|Calymmian|Calymmian|Coompana Province. A-type or transitional A-type; greenschist to lower amphibolite facies. Significant crustal source component and parts with an upwelled asthenospheric mantle component. Similar rocks were intersected in the Mallabie 1 drillcore in SA. Slightly younger than the Bunburra Suite. Report includes lithologic/petrographic description, structural analysis, whole-rock geochemistry, geochronology, Sm-Nd, Lu-Hf. Also p: ~101-117, 123-125, 128, 133-135, 142.42.|1499-1479 Ma)||||Metagranites including metamonzogranites, metamonzodiorite and metasyenite. Also contains mafic schist and a grey schist interpreted as a metarhyolite. Includes porphyritic monzogranite gneiss interlayered with the metatonalite, metasyenogranite.|
79175|Undawidgi Supersuite|73091|5|Briefly described|map legend|Calymmian|Calymmian||C. 1500-1530 Ma||Includes the Gilgerabbie Suite.||Granitic gneiss.|30-NOV-21
79175|Undawidgi Supersuite|73224|5|Briefly described|p42, p44|Calymmian|Calymmian|Coompana Province, western. A-type. Product of intracontinental extension following cessation of subduction. Represents recycling of the c. 1600 Ma arc crust with additional juvenile mantle input.|c. 1505-1487 Ma||Gilgerabbie Suite|||
79175|Undawidgi Supersuite|73225|5|Briefly described|p3, 4, 18, p22 Fig.10|||Coompana Province. West of the Mulyawarra Shear Zone. Formed by recycling of c.1600 Ma arc crust, with additional juvenile mantle input,  in a rift setting.|c.1505-1487 Ma.||Gilgerabbi Suite||Bimodal; A-type.|
79175|Undawidgi Supersuite|73641|6|Mentioned|p4||||||Gilgerabbie Suite|||
39512|Underwood Gneiss|63417|5|Briefly described|Map legend|Archean|Archean|Of the Callina Supersuite. Age: c. 3462 Ma. Geological Province: Pilbara Craton. Banded tonalite, granodiorite and monzogranite, gneiss and migmatite; strongly sheared; S-C mylonite fabric.||||||15-APR-13
39512|Underwood Gneiss|63441|5|Briefly described|p7 Tb. 2|Archean|Archean|Of the Callina Supersuite. Age: >c. 3462 Ma. Geological Province: Pilbara Craton.||||||15-APR-13
39512|Underwood Gneiss|64621|5|Briefly described|Map legend|Archean|Archean|Of the Callina Supersuite. Age: c. 3464 Ma. Banded tonalite, granodiorite and monzogranite gneiss and migmatite; strongly sheraed.||||||15-APR-13
39512|Underwood Gneiss|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||Of Mount Edgar Granitoid Complex.|||Mixed felsic-mafic banded gneiss and migmatite, tonalite, granodiorite, and monzogranite bodies; local amphibolite xenoliths and pods; strongly sheared, C-S mylonite fabric.|
39512|Underwood Gneiss|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|>3462 Ma.|Of Callina Supersuite.|||Banded tonalite, granodiorite, and monzogranite gneiss and migmatite; strongly sheared, S-C mylonite fabric.|
39512|Underwood Gneiss|65827|2|Defined|p6 Tb.2, p12 Tb.3, p18-19, p22-24,p59-60|Paleoarchean|Paleoarchean|New name; after Underwood Well.  c.3350-3325 Ma metamorphism and partial melting.   Underwood Gneiss protoliths were probably intruded by Fig Tree Gneiss protoliths: their contact is now sheared. Corresponds in part to Mount Edgar Mylonite Complex.|>3462 Ma protoliths.|Of Callina Supersuite.||Intruded by Kennell, Chessman, Wilina Granodiorites. Faulted but concordant contact with Duffer Formation.|Mixed felsic-mafic quartzofeldspathic banded gneiss, with characteristic foliated discordant metamorphosed gabbro-diorite bodies and amphibolite dykes; thin concordant gneissic tonalite, granodiorite and monzogranite bodies.|21-MAY-14
39512|Underwood Gneiss|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Callina Supersuite. Banded tonalite, granodiorite, and monzogranite gneiss and migmatite; strongly sheared.||||||
39512|Underwood Gneiss|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Callina Supersuite|||Banded tonalite, granodiorite, and monzogranite gneiss and migmatite; strongly sheared|
39512|Underwood Gneiss|69566|6|Mentioned|p236|||Mount Edgar Granitoid Complex, East Pilbara Granite-Greenstone Terrane.||Callina Supersuite.||||
39512|Underwood Gneiss|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3493-3462 Ma (inferred)|Unit of Callina Supersuite.|||Banded tonalite, granodiorite, and monzogranite gneiss and migmatite; strongly sheared|
39512|Underwood Gneiss|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||felsic gneiss|
39512|Underwood Gneiss|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|||Callina Supersuite|||Granitic gneiss and migmatite; metatonalite, metagranodiorite, and metamonzogranite banding; strongly sheared.|
69697|Upper Nickol Suite|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Age: 3024-3012Ma. Geological Province: Pilbara Craton.  See also p54-55 Fig. 3. Probably named for upper part of Nickol River?||||||07-NOV-08
27598|Van Emmerick Conglomerate|24061|6|Mentioned|p175|||Geological Province:  Canning Basin.||||||
27598|Van Emmerick Conglomerate|30097|6|Mentioned|Table 25|||||||||
27598|Van Emmerick Conglomerate|30525|6|Mentioned|Map legend|Frasnian|Givetian|Frasnian? to Givetian?||||||
27598|Van Emmerick Conglomerate|30533|4|Described|p24|||On Table 6||||||
27598|Van Emmerick Conglomerate|30896|4|Described|p19|||||||||
27598|Van Emmerick Conglomerate|31226|6|Mentioned|Map legend|Frasnian|Givetian|Givetian? to Frasnian?||||||
27598|Van Emmerick Conglomerate|31332|6|Mentioned|Fig. 3|||||||||
27598|Van Emmerick Conglomerate|31870|6|Mentioned|p8|||||||||
27598|Van Emmerick Conglomerate|35104|6|Mentioned|Fig.8|||||||||
27598|Van Emmerick Conglomerate|36890|4|Described|p335|||||||||
27598|Van Emmerick Conglomerate|40793|6|Mentioned|p163|||||||||
27598|Van Emmerick Conglomerate|41023|6|Mentioned|Fig.3|||||||||
27598|Van Emmerick Conglomerate|41215|6|Mentioned|p263|||||||||
27598|Van Emmerick Conglomerate|42030|6|Mentioned|p748|||||||||
27598|Van Emmerick Conglomerate|42564|5|Briefly described|p10|||||||||
27598|Van Emmerick Conglomerate|42710|5|Briefly described|map legend|Late Devonian||||||||
27598|Van Emmerick Conglomerate|42811|5|Briefly described|p42|||||||||
27598|Van Emmerick Conglomerate|42860|5|Briefly described|Fig.2|||||||||
27598|Van Emmerick Conglomerate|43281|6|Mentioned|Map legend|Late Devonian|Late Devonian|Canning Basin.||||||
27598|Van Emmerick Conglomerate|43666|6|Mentioned|p22|||||||||
27598|Van Emmerick Conglomerate|43818|6|Mentioned|Table 2,p42|||||||||
27598|Van Emmerick Conglomerate|44998|14|Not recorded|p26,43|||(E51-8,7).||||||
27598|Van Emmerick Conglomerate|45101|6|Mentioned|Fig.8|||||||||
27598|Van Emmerick Conglomerate|45153|3|Fully described|App.3-53|||See also App.2-28||||||
27598|Van Emmerick Conglomerate|48931|5|Briefly described|p61|||||||||
27598|Van Emmerick Conglomerate|64580|6|Mentioned|map legend|||Frasnian and Famennian conglomerates associated with Devonian reef complexes.||||||15-DEC-08
27598|Van Emmerick Conglomerate|65486|6|Mentioned|p12, p35 Fig.47|Devonian|Devonian|Canning Basin. Well-developed tree cover is the result of higher rainfall.||||||
27598|Van Emmerick Conglomerate|66127|3|Fully described|pp146-149, pp379-381. |Famennian|Frasnian|Of Guppy et al. (1958). Type section is on eastern edge of Van Emmerick Range. Northern Lennard Shelf. Forms Wunala Hill and a smaller body NW of Hawkstone Creek. Thickness probably >300 m. An Upper Van Emmerick Conglomerate unit is mapped separately and dated as probably Famennian. Is said to extend into the Givetian in subsurface.||||Interfingers with Pillara Limestone and Napier Formation.|Polymictic pebble and boulder conglomerate, with lesser intercalated coarse-grained poorly-sorted sandstone; up to 95% granitic clasts; alluvial-fan, fan-delta, and submarine-fan deposits.|
27598|Van Emmerick Conglomerate|69099|4|Described|GEOL_LUT_CSV files + geochron files|Famennian|Frasnian|Lennard Shelf. Canning Basin. Frasnian and Famennian conglomerates associated with Devonian reef complexes. See info in 500k_geologyp08_lut.csv|||||Siliciclastic cobble to boulder conglomerate, minor sandstone and interbedded limestone; Frasnian and Famennian platform- to basin-level conglomerates associated with carbonate reef complexes.|04-AUG-15
27598|Van Emmerick Conglomerate|69165|6|Mentioned|500k_geologyp08_lut.csv|Famennian|Frasnian|||||||
27598|Van Emmerick Conglomerate|69634|4|Described|GEOL_LUT_CSV files|Famennian|Frasnian|Of Lennard Shelf, Canning Basin.  Frasnian and Famennian platform- to basin-level conglomerates associated with carbonate reef complexes. Events: Alice Springs Orogeny. See 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|372.2-358.9 Ma (inferred)||||Siliciclastic cobble to boulder conglomerate, minor sandstone and interbedded limestone|
27598|Van Emmerick Conglomerate|69660|5|Briefly described|Map legend|Famennian|Frasnian|Canning Basin. Frasnian and Famennian platform- to basin-level conglomerates associated with carbonate reef complexes.|||||Siliciclastic cobble to boulder conglomerate, minor sandstone and interbedded limestone.|
27598|Van Emmerick Conglomerate|70154|4|Described|100k_interpgeop_lut.csv|Famennian|Frasnian|See also 250k_interpgeop_lut.csv.|359-372 Ma||||Siliciclastic cobble to boulder conglomerate, minor sandstone and interbedded limestone; Frasnian and Famennian platform- to basin-level conglomerates associated with carbonate reef complexes|
27598|Van Emmerick Conglomerate|71267|4|Described|GEOL_LUT_CSV files|Famennian|Frasnian|Of Lennard Shelf, Canning Basin. Events: Meda Transpression (323-310 Ma); Red Bluffs Extension (372.2-360 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma); Pillara Movement (Alice Springs Orogeny phase 2) (390-360 Ma); Van Emmerick Extension (382.7-372.2 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|372.2-358.9 Ma (inferred)||||Massive boulder fanglomerate at the base with mainly quartzite and sandstone clasts up to 1m in a granitoid-derived matrix, overlain by mixed fluviatile to deltaic conglomerate and sandstone; with granitoid, schist and felsic volcanic clasts|
34566|Vasse Group|22820|5|Briefly described|p10 Fig.4|Late Permian|Late Permian|Term may be an informal compound term for part of the Vasse River Coalfield? - the section it covers is equivalent to the Sue Group units.||||||12-AUG-08
79360|Vetters Subgroup|71270|5|Briefly described|GEOL_LUT_CSV files|||Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.||Unit of Kalgoorlie Group.|Includes Bent Tree Basalt, Big Dick Basalt, Missouri Basalt, Siberia Komatiite, Victorious Basalt, Walter Williams Formation, Wongi Basalt.|||
79360|Vetters Subgroup|72095|6|Mentioned|p5 Fig 3|Neoarchean|Neoarchean|Eastern Goldfields, Yilgarn Craton.||Unit of Kalgoorlie Group.||||
24063|Victorious Basalt|22534|4|Described|p15-16, Fig.4 p7|||of Grants Patch Group. See also p9||||||
24063|Victorious Basalt|22596|6|Mentioned|Fig.9 p419|||||||||
24063|Victorious Basalt|22856|6|Mentioned|p434|||Host of primary Au deposit||||||
24063|Victorious Basalt|42156|6|Mentioned|Fig.1 p373|||||||||
24063|Victorious Basalt|42221|5|Briefly described|Table 1 P6|||||||||
24063|Victorious Basalt|42382|5|Briefly described|p21|||||||||
24063|Victorious Basalt|42436|5|Briefly described|Fig.2 P.75|||||||||
24063|Victorious Basalt|42696|6|Mentioned|Plate 1B|||||||||
24063|Victorious Basalt|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
24063|Victorious Basalt|42870|5|Briefly described|Table 1, P67|||||||||
24063|Victorious Basalt|42989|5|Briefly described|Table 1,Fig.2|||||||||
24063|Victorious Basalt|43074|6|Mentioned|Fig.6.|||||||||
24063|Victorious Basalt|43101|5|Briefly described|Table 1.|||of Grants Patch Group||||||
24063|Victorious Basalt|43102|5|Briefly described|p8|||||||||
24063|Victorious Basalt|43162|6|Mentioned|5|||||||||
24063|Victorious Basalt|43496|6|Mentioned|6|||||||||
24063|Victorious Basalt|50551|5|Briefly described|p1092 Fig.3||Archean|Plagioclase-phyric series of several lava flows vary from fine grained-glassy pillow basalt to coarse non-pillowed flows. Parent: Grants Patch Group||||||07-NOV-08
24063|Victorious Basalt|60076|5|Briefly described|p12 Tb. 2|||Porphyritic basalt.  Max. thickness: <3000m.  Geological Province: Ora Banda domain (Yilgarn Craton).||||||02-FEB-05
24063|Victorious Basalt|60514|5|Briefly described|p61, p64, p65, p64 Fig. 5|Archean|Archean|Of the Grants Patch Group. Geometrically overlays the Black Flag succession. Maximum thickness: 100m. Feldspar-phyric tholeiitic basalt. Geological Province: Yilgarn Craton.||||||07-FEB-11
24063|Victorious Basalt|60627|5|Briefly described|p61, p65 Tb.1|||Plagioclase-phyric basalt. Of Grants Patch Group.||||||
24063|Victorious Basalt|65204|6|Mentioned|pg6 Tbl.1, p11|Archean|Archean|Of Grants Patch Group. Coarsely plagioclase-phyric basalt; similar to Burbanks Formation S of Coolgardie.||||||
24063|Victorious Basalt|65834|6|Mentioned|p7, 13, 38, 41|||Mount Pleasant district, Ora Banda Domain, Kalgoorlie Terrane. Hosts the Racetrack gold deposit.||Grants Patch Group.|||Massive to pillowed, coarsely plagioclase-phyric tholeiitic basalt, locally with a coarse-grained doleritic groundmass.|
24063|Victorious Basalt|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2726 - 2680 Ma (inferred).|Kalgoorlie Group|||Porphyritic basalt; plagioclase-phyric; massive to pillowed; metamorphosed.|
24063|Victorious Basalt|70326|4|Described|p360-362|Neoarchean|Neoarchean|Geological province: Ora Banda region, Ora Banda Domain, Kalgoorlie Terrane, Yilgarn Craton. ||||Overlain by Ora Banda Sill. Underlain by Bent Tree Basalt. Correlable to White Hope Basalt.|Feldspar megacrystic basalt.|
24063|Victorious Basalt|71166|5|Briefly described|p9 fig 3.4a, p19, p20 fig 3.13, p26|||Hosts shallow gold mineralisation. ||||Overlies the Bent Tree Basalt.|Porphyritic basalt.|
24063|Victorious Basalt|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).  See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2726-2680 Ma (inferred)|Unit of Vetters Subgroup.|||Porphyritic, plagioclase-phyric basalt; massive to pillowed; metamorphosed|
24063|Victorious Basalt|72814|5|Briefly described|p201, Fig. 3, p202 Fig. 4, p204, p205|||East of Zuleika Shear, Ora Banda Domain.Mineralised.|||||Coarse plagioclase porphyritic basalt.|
24063|Victorious Basalt|73391|5|Briefly described|p20, 51, 53-55, 58, 75, 78, 80, 88, 178|||See also p194, 238, 244, 252, 254-255, 266-267, 271-272, 279, 310, 324-326, 329-331, 343-344, 362-365, 443, Appendices. Ora Banda Domain, Eastern Goldfields Province. This is described as the upper of two tholeiitic mafic flows (separated by a thin discontinuous horizon of carbonaceous shale) of the Upper Basalt. 1000m thick.||Grants Patch Group; Upper Basalt.||Overlies Bent Tree Basalt. Is overlain by Ora Banda Sill, Spargoville Formation, Talbot formation, Centenary Shale and White Flag Formation.|A distinctive coarse plagioclase-phyric (locally highly stretched), tholeiitic mafic flow sequence. Well-developed volcanic features include pillow margins, hyaloclastite breccia, interflow sedimentary rocks.|
24063|Victorious Basalt|73596|6|Mentioned|p1160|||Appears as Victorious/Paringa Basalt.||||||
30170|Victory Dolerite|23137|4|Described|p245 Table.2|||||||||
30170|Victory Dolerite|43102|6|Mentioned|p8|||Of Devon Consols Basalt?||||||
30170|Victory Dolerite|43162|6|Mentioned|5|||U-Pb Age: 2693+/-50Ma||||||
30170|Victory Dolerite|60514|5|Briefly described|p28|Archean|Archean|Of the Devon Consol Basalt. Is internally zoned, with an ultramafic pyroxenite base to ophitic gabbro. Xenocrystic zircons older than 3400-3100 Ma (Compston et al., 1986; Claoue'-Long et al., 1988). Geological Province: Yilgarn Craton.||||||07-FEB-11
30170|Victory Dolerite|60623|5|Briefly described|p28|Archean|Archean|Of Devon Consols Basalt||||||07-NOV-08
30170|Victory Dolerite|70326|5|Briefly described|p360,363|Neoarchean|Neoarchean|Geological province: Kambalda Domain, Kalgoorlie Terrane, Yilgarn Craton.||||Intrudes into Devon Consols Basalt.||
30170|Victory Dolerite|73596|6|Mentioned|p1161|Neoarchean|Neoarchean|Kalgoorlie area.|2669 +/- 11 Ma.|||Intrudes Black Flag Group. Correlated with Mount White Dolerite.||
24064|Vincent Member|41831|5|Briefly described|p557|||See also Fig.3||||||
24064|Vincent Member|43297|6|Mentioned|p18|||Rottnest Island.||||||
24064|Vincent Member|43504|6|Mentioned|14||Quaternary|Age: 3000-6000 Years BP||||||
35793|Vines Formation|24161|5|Briefly described|p9 Fig.6|||Unconformably overlies the Wahlgu Formation. Unconformably overlain by the Table Hill Volcanics. Geological Province: Officer Basin.||||||
35793|Vines Formation|50085|5|Briefly described|p11 Fig. 6|Cambrian|Neoproterozoic|Age: ~540Ma.  Geological Province: Officer Basin.||||||
35793|Vines Formation|50205|5|Briefly described|p59 Fig.1|Fortunian|Neoproterozoic|Of Officer Basin.||||||
35793|Vines Formation|61023|5|Briefly described|p13, p15 Fig. 8|Early Cambrian|Early Cambrian|Geological Province: Officer Basin.||||||11-APR-08
35793|Vines Formation|62453|3|Fully described|p5 Fig. 3, 50|Cambrian|Cambrian|Geological Province: Officer Basin. Correlates with Mount Currie Conglomerate. Sandstone, diamictite, siltstone, shale, mudstone, conglomerate, minor carbonates and evaporites.||||||
35793|Vines Formation|62987|5|Briefly described|p30|||Thick conglomeratic unit. Was originally considred to be earliest Cambrian in age but this is now in doubt. It may relate to the Wahlgu and Lungkarta Formations.||||||
35793|Vines Formation|64103|2|Defined|p397, p399 Fig. 2, p400 Fig. 3, p401|Early Cambrian|Late Ediacaran|Includes six informal units. Depositional env in present study is fluvial stream flow. Geological Province: Officer Basin. See p406 for detailed info. Fluvial pebble conglomerate.||||||03-SEP-14
35793|Vines Formation|64325|5|Briefly described|p82 Fig. 2, p85|Early Cambrian|Neoproterozoic|A unit of Supersequence 4. Age: ~545Ma. Geological Province: western Officer Basin. Sandstone unit deposited syntectonically with the uplift of the Musgrave Complex during Petermann Ranges Orogeny.||||||03-SEP-14
35793|Vines Formation|65363|6|Mentioned|p5 Fig.4. |Cambrian|Cambrian|||||||
35793|Vines Formation|65385|6|Mentioned|pS133|||Of Officer Basin. U-Pb detrital zircon age (from sandstone) of 973+/-21 Ma (Nelson, 2002).||||||08-MAR-12
35793|Vines Formation|67195|5|Briefly described|p10 fig 6, p19 tbl 1, p40, 47, 53|Cambrian|Neoproterozoic|Western Officer Basin. Thermal conductivity of 2.69 W/mK. Basal unit of one well in this study. See also App 1.|||||Diamictite.|
35793|Vines Formation|69003|6|Mentioned|p60|Cambrian|Cambrian|Officer Basin.||||||
35793|Vines Formation|69029|6|Mentioned|p329|Cambrian|Neoproterozoic|Of Officer Basin.||||Overlain unconformably by Table Hill Volcanics. Underlain unconformably by Wahlgu Formation.||
35793|Vines Formation|71800|6|Mentioned|p26-p27|Early Cambrian|Ediacaran|Officer Basin.||||Overlies the McFadden Formation.|Sandstone and gritty sandstone.|
24065|Vittoria Member|40314|4|Described|Table 1|||||||||
24065|Vittoria Member|40367|4|Described|p81|Holocene|Holocene|Of Safety Bay Sand. Overlies Burragenup and Rosamel Members (sharp contact). Modern beach ridge/dune sequence of partly indurated, root-casted and calcreted sediment of the older members of the unit, truncated by a humic soil over which this member rests.||||||07-AUG-07
24065|Vittoria Member|69788|5|Briefly described|p1027, p1029-1030, p1032-1035|Holocene|Holocene|Semeniuk (1983). Occurs as dunes up to 20m tall, and as a sand sheet. Still mobile: blown northwards by wind up to 16m per year. Contains the highest amounts of aragonite and high-Mg calcite in the study area and probably represents the original composition of older calcarenite members of Tamala Limestone.||Uppermost unit in Safety Bay Sand.||Overlies Burragenup Member and most Members of Tamala Limestone.|Loose, calcareous mobile sand: fine- to medium-grained, well-sorted carbonate bioclasts, quartz and feldspar grains.|
24065|Vittoria Member|69840|5|Briefly described|p188, p186 Fig.3, p196 Fig.13, p197|Holocene|Holocene|Age given as recent.||Safety Bay Sand||Overlies Cooloongup Sand.|c. 35% aragonite remaining calcite.|
77944|Vivien Formation|69583|5|Briefly described|p39-40, p88-89, p171|||Crops out in the Mount White Syncline. Geochronology by Kositcin et al. (2008).|c.2692 Ma (maximum depositional age).||||A succession of feldspathic, volcaniclastic sedimentary rocks.|
77944|Vivien Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Stated to include Mosquito Well Conglomerate. [If so, this latter needs to be renamed the Mosquito Well Conglomerate Member].|2690 - 2660 Ma (inferred).|Mount White Group|||Felsic volcaniclastic rock, volcanolithic sandstone, and siltstone; metamorphosed.|
77944|Vivien Formation|70326|4|Described|p336-337,339|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton. [Also referred to as Vivien Metasediments on p336]. In contact with the Turrett Dolerite via sheared unconformity. Intrudes into White Hope Basalt.|Max dep age: 2686+\-7 Ma (Squire et al., 2010).||Includes Mosquito Well Conglomerate.|Correlable to Black Flag Group. Underlain unconformably by Turret Dolerite.|Weakly metamorphosed polymictic conglomerate, fine- to coarse-grained sandstone, chert, basalt and dolerite.|
77944|Vivien Formation|71212|5|Briefly described|intro p2|||Yilgarn Craton. ||Mount White Group|Includes the Mosquito Well Conglomerate Member|||
77944|Vivien Formation|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2690-2662 Ma (inferred)|Unit of Mount White Group.|||Felsic volcaniclastic rock, volcanolithic sandstone, and siltstone; metamorphosed|
77944|Vivien Formation|71310|5|Briefly described|p774, p776 Fig.8, p778, p783-784, p786|||Agnew-Wiluna greenstone belt. Folding described.|c.2686 Ma.||||Volcanisedimentary rocks.|
77944|Vivien Formation|73151|4|Described|p1-6, p9 Fig.5, p11-16|Neoarchean|Neoarchean|Yilgarn Craton, Kalgoorlie Terrane, Agnew Greenstone Belt. Lower unit of the Mount White Group. Limited distribution of conglomerates, clasts are derived from the uppermost units of the Kalgoorlie Group (Turret Dolerite, White Hope Basalt, Redeemer Basalt). Rounded felsic-intermediate clasts derived from a volcanic source emergent above sea level. Low-energy pelagic to hemipelagic sedimentation in water depth of at least 50 m with debris flows and turbidity currents. Represents subaqueous ring-plain surrounding a volcanic island and uplift of the underlying Kalgoorlie Group above sea level, redeposited as mass flows into a subaqueous environment.|ca. 2690-2670 Ma|Mount White Group|Mosquito Well Conglomerate Member|Unconformably overlies and faulted against Kalgoorlie Group, conformably underlies Maria Mine Formation, Halfway Well Basalt.|Predominantly polymictic conglomerate, fine- to coarse-grained sandstone, chert. The conglomerate is massive, poorly sorted, clast-supported and contains a sandy matrix, dominantly mafic to felsic volcanic clasts are sub-rounded to well-rounded.|
77944|Vivien Formation|73596|5|Briefly described|p1152, 1154, 1156-1160, 1162|Neoarchean|Neoarchean|Agnew-Wiluna Greenstone Belt. Occupies the keel of the Mount White Syncline. Ring-plain and submarine aprons surrounding emergent volcanic islands. Inherited zircons aged 2806 +/- 7 Ma and 2798 +/- 13 Ma.|2678 +/- 4 Ma (MDA).|Mount White Group.|Mosquito Well Conglomerate Member.|Overlies White Hope Basalt (Two Sisters Subgroup). Is overlain conformably by Halfway Well Basalt. Correlated with Black Flag Group.|Mainly felsic volcanoclastic rocks, sandstones, siltstones and argillites. Abundant felsic fragmental rocks.|
27601|Vlaming Sandstone|23726|5|Briefly described|p88|Middle Miocene|Late Oligocene|Of Cape Range Group. Overlying unit Exmouth Sandstone. Underlying unit Pilgramunna Formation. Geological Province: Carnarvon Basin.||||||20-DEC-06
27601|Vlaming Sandstone|32750|6|Mentioned|p311|||Refers Condon (1968)||||||
27601|Vlaming Sandstone|33593|6|Mentioned|p107|||||||||
27601|Vlaming Sandstone|35105|6|Mentioned|Fig.5|||||||||
27601|Vlaming Sandstone|36257|6|Mentioned|Table 2.1|||||||||
27601|Vlaming Sandstone|37016|6|Mentioned|Map legend|middle Miocene|middle Miocene|||||||
27601|Vlaming Sandstone|39427|4|Described|Table 1|||||||||
27601|Vlaming Sandstone|41271|3|Fully described|p186|||Of Cape Range Group.||||||
27601|Vlaming Sandstone|41438|6|Mentioned|p111|||||||||
27601|Vlaming Sandstone|42116|6|Mentioned|p69|||||||||
27601|Vlaming Sandstone|45015|5|Briefly described|map legend|Tertiary|Tertiary|Of the Yardie Group. Age is Late Tertiary.||||||01-JUN-06
27601|Vlaming Sandstone|46983|6|Mentioned|Fig.2|||||||||
27601|Vlaming Sandstone|61155|5|Briefly described|p15|Middle Miocene|Middle Miocene|Of the Cape Range Group. Overlies and interfingers with Pilgramunna Formation. Age: 12-~10Ma. Thickness: 35m. Geological Province: Carnarvon Basin /onshore and offshore.||||||
27601|Vlaming Sandstone|61958|5|Briefly described|Map sheet 1|Neogene|Neogene|Of the Yardie Group.||||||
27601|Vlaming Sandstone|66125|5|Briefly described|p133 Fig.4|||Ningaloo Reef area; onshore.||||Overlies Pilgramunna Formation.|Medium-grained aeolian deposits.|
27601|Vlaming Sandstone|67200|5|Briefly described|p8 fig 6, |Miocene|Oligocene|||||Overlies Pilgramunna Formation, overlain by Exmouth Sandstone|Planar cross bedded sandstone.|
27601|Vlaming Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||calcarenite|
29102|Volpress Member|41199|4|Described|p12|||Reserved as Volpress. Of Menzies Formation.||||||
79289|Voodoo Child Formation|69595|5|Briefly described|p6, p35, p36|Paleoproterozoic|Paleoproterozoic|Tropicana Zone. |||||Dacitic rocks and mafic to ultramafic rocks.|
79289|Voodoo Child Formation|70089|6|Mentioned|p263|Paleoproterozoic|Paleoproterozoic|Tropicana Zone, NE Albany-Fraser Orogen.|||||Dacite; interlayered mafic to ultramafic intrusive rocks.|
79289|Voodoo Child Formation|70090|6|Mentioned|p457|||Comprises dacitic rocks.||||||
79289|Voodoo Child Formation|70182|6|Mentioned|p3-4|||Albany-Fraser Orogen. Said to be "associated with" the McKay Creek Metasyenogranite.||||||
79289|Voodoo Child Formation|70256|5|Briefly described|p4-5, p24, p28|||Less (2013). Volcanosedimentary and intrusive rocks, formed in a small pull-apart basin. Emplaced during the c.1770 Ma Ngadju Event.|c.1760 Ma.||||Dacite; interlayered leucogabbro and mafic-ultramafic intrusive rocks.|
79289|Voodoo Child Formation|70802|5|Briefly described|250k_pre_mesozoic_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Tropicana Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage II (1225-1140 Ma); Albany-Fraser Orogeny (1330-1140 Ma); Albany-Fraser Orogeny Stage I (1330-1260 Ma); Biranup Orogeny (1710-1620 Ma); Ngadju Event (1780-1760 Ma).|1780-1700 Ma (inferred)||||Interlayered mafic to ultramafic intrusive rocks, metabasalt to metadacite volcanic rocks, and metasedimentary rocks; may include Paleoproterozoic metagranite|
79289|Voodoo Child Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Tropicana Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen. Age inferred.||||Remnants included in McKay Creek Metasyenogranite.|Interlayered mafic to ultramafic intrusive rocks, metabasalt to metadacite volcanic rocks, and metasedimentary rocks; may include Paleoproterozoic metagranite.|
29721|Wadarrah Quartz Monzonite|7471|5|Briefly described|p7, Map legend|Archean|Archean|Mis-spelt as Wandarrah on p7.|||||Hornblende-quartz monzonite.|
29721|Wadarrah Quartz Monzonite|23281|6|Mentioned|p7|||||||||
29721|Wadarrah Quartz Monzonite|23591|5|Briefly described|p17|Archean|Archean|2643+/-6 Ma (SHRIMP U-Pb zircon). Geological Province: Yilgarn Craton.||||||07-NOV-08
29721|Wadarrah Quartz Monzonite|23611|5|Briefly described|p18|Archean|Archean|Age: 2644+/-13 Ma. See also page 32 Appendix 1. Geological Province: Yilgarn Craton.||||||07-NOV-08
29721|Wadarrah Quartz Monzonite|23930|5|Briefly described|p131|Archean|Archean|Geological Province: Yilgarn Craton. Age: 2643+/-6Ma.||||||07-NOV-08
29721|Wadarrah Quartz Monzonite|24135|6|Mentioned|p7 Fig. 3|||||||||
29721|Wadarrah Quartz Monzonite|24174|4|Described|p16-17|Archean|Archean|Age: 2643+/-6 Ma (U-Pb zircon).  Geological Province: Eastern Goldfields.||||||23-OCT-14
29721|Wadarrah Quartz Monzonite|43289|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
29721|Wadarrah Quartz Monzonite|60981|5|Briefly described|p175 Fig.1|Archean|Archean|Age: 2643 +/- 6 Ma. Geological Province: Yilgarn Craton.||||||07-NOV-08
29721|Wadarrah Quartz Monzonite|64586|5|Briefly described|Map legend|Archean|Archean|Hornblende-quartz monzonite with local platy alignment.||||||07-NOV-08
29721|Wadarrah Quartz Monzonite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Hornblende-bearing quartz monzonite with local platy mineral alignment.|07-AUG-15
29721|Wadarrah Quartz Monzonite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Hornblende-bearing quartz monzonite with local platy mineral alignment.|
29721|Wadarrah Quartz Monzonite|71270|4|Described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton.|||||Hornblende-bearing quartz monzonite with local platy mineral alignment|
33982|Wade Creek Formation|24503|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Sandstone, pebbly sandstone, conglomerate, siltstone and mudstone. Geological Province: Victoria River  Basin.||||||19-MAY-15
33982|Wade Creek Formation|63866|5|Briefly described|p129-p130, p137|||Victoria River Basin.||||||
33982|Wade Creek Formation|64580|4|Described|map legend|Mesoproterozoic|Paleoproterozoic|Sandstone, pebbly sandstone, conglomerate, siltstone, and mudstone.||||||15-DEC-08
33982|Wade Creek Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Victoria River Basin|||Includes Mount John Shale Member and two unnamed members.||Fine- to coarse-grained quartz sandstone, lithic quartz sandstone, pebbly sandstone, conglomerate, siltstone, and mudstone; also ferruginous chert breccia member.|04-AUG-15
33982|Wade Creek Formation|69165|4|Described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|See also 500k_interpgeop_lut.csv. |||Includes Mount John Shale Member||Fine- to coarse-grained quartz sandstone, lithic quartz sandstone, pebbly sandstone, conglomerate, siltstone, mudstone and stromatolitic chert.|
33982|Wade Creek Formation|69634|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Halls Creek Orogen. Of Victoria River Basin. Events: Alice Springs Orogeny; Yampi Orogeny D1/M1. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|1600-1000 Ma (Inferred)||Includes Mount John Shale Member.||Fine- to coarse-grained quartz sandstone, lithic quartz sandstone, pebbly sandstone, conglomerate, siltstone, and mudstone, chert breccia; angular to rounded chert fragments in a ferruginous chert-sandstone matrix|
33982|Wade Creek Formation|70154|4|Described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|See also 500k_interpgeop_lut.csv.|1000-1600 Ma||||Fine to coarse grained quartz sandstone, lithic quartz sandstone, pebbly sandstone, conglomerate, siltstone and thin bedded sandstone. Chert Breccia; angular to rounded chert fragments in a ferruginous chert-sandstone matrix.|
33982|Wade Creek Formation|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Osmond Basin.||||||
33982|Wade Creek Formation|71267|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Halls Creek Orogen. Of Osmond Basin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|1600-1000 Ma (inferred)||Includes Mount John Shale Member.||Fine- to coarse-grained quartz sandstone, lithic quartz sandstone, pebbly sandstone, conglomerate, siltstone, and mudstone, Chert breccia; angular to rounded chert fragments in a ferruginous chert-sandstone matrix|
33982|Wade Creek Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Osmond Basin.|||||Fine- to coarse-grained quartz sandstone, lithic quartz sandstone, pebbly sandstone, conglomerate, siltstone, and mudstone.|
74204|Wadeye Group|61542|4|Described|p276, p277 Fig. 2, p286|Westphalian|Namurian|Includes Point Spring Sandstone (formerly part of Weaber Group), Arco and Aquitaine Formations. Overlies Weaber Group; unconformably overlain by Kulshill Group. Geological province: Bonapart Basin/Petrel-Sub-basin.||||||07-FEB-11
74204|Wadeye Group|64630|5|Briefly described|p31 Fig.2, p37|Bashkirian|Serpukhovian|Province: Bonaparte Basin. Underlies the Kulshill Group, unconformably overlies the Weaber Group. Palynology age: S. ybertii.||||||18-JAN-10
74204|Wadeye Group|69452|4|Described|p36:4-5, 9, 11-12, 14-15, 17-18|Carboniferous|Carboniferous|Gorter et al. (2005). Gorter et al. (2008) referred to this succession as the Wadeye Sub-group and recommended it be included in the overlying Kulshill Group; this is not [?yet] the case. Petrel Sub-basin, Bonaparte Basin. Outcrops identified as Border Creek Member in AUVERGNE are no longer assigned to this Group. Late Mississippian to Early Pennsylvanian.|||Arco, Aquitaine Formations; Point Spring Sandstone.|Unconformably overlies Weaber Group. Is overlain unconformably by Kulshill Group.|Siltstone, shale, sandstone.|12-JUL-16
74204|Wadeye Group|69653|6|Mentioned|p10, 14|Carboniferous|Carboniferous|Petrel Sub-basin.|||Arco, Aquitaine Formations.|Overlies Weaber Group. Is overlain by Kulshill Group.||
74204|Wadeye Group|69673|6|Mentioned|p167, p170 fig 142 p171, p172|Carboniferous|Carboniferous||||Includes Arco Formation, Aquitaine Formation|Overlies Kingfisher Shale, overlain by Kuriyippi Formation, unconformably overlain by Kulshill Group||
74204|Wadeye Group|70061|5|Briefly described|Petrel Sub-basin Fig.3|Bashkirian|Serpukhovian|See also Regional geology: Fig.8, p5.|||Arco and Aquitaine Formations.|Overlies Weaber Group. Is overlain by Kulshill Group.||12-JUL-16
74204|Wadeye Group|71146|5|Briefly described|p6|Serpukhovian|Serpukhovian|Bonaparte Basin.||||Unconformably overlies the Weaber Group.|Mixed sandstone, mudstone and coal.|
74204|Wadeye Group|71267|5|Briefly described|1M_geologyp12_lut.csv||||||Includes Border Creek Formation, Point Spring Sandstone.|||
74204|Wadeye Group|73117|6|Mentioned|p11, p15, p31|Bashkirian|Serpukhovian|Bonaparte Basin. Approximately coeval with Reeves Formation. Lies below coarse siliciclastic facies with a 'possible glacial fingerprint'. Contains facies unlikely to yield conodonts. Palynozonation: S. ybertii.|||Aquitaine Formation, Arco Formation.|||
74204|Wadeye Group|73184|6|Mentioned|p200, p201 Fig.12|||Bonaparte Basin, southeast. Possibly glaciogenic.||||||
24067|Wadjemup Formation|41751|2|Defined|p7|Pliocene|Miocene|Age: late Miocene to Pliocene||||||
24067|Wadjemup Formation|44144|4|Described|p502 Tb.4-21, p518 fig 4-162, p520|Pliocene|Late Miocene|Type Section: Gage Roads 1 well (100-389m). 289m thick marine shelf deposits.||||Overlies Stark Bay Formation unconformably.  Overlain by Tamala Limestone.|Yellow to red, well-sorted medium- to coarse-grained calcarenite; some limestone and dolomite.|
24067|Wadjemup Formation|61155|5|Briefly described|p15|Late Pliocene|Late Miocene|Age: 5-3Ma. Thickness: 200m. Interfingers with Yoganup Formation. Geological Province: Perth Basin.||||||
26193|Wagina Sandstone|12758|5|Briefly described|p9|Late Permian - Correct|Late Permian - Correct|Unconformably overlain by Kockatea Shale. Geological Province: Northern Perth Basin.||||||11-APR-08
26193|Wagina Sandstone|15881|6|Mentioned|p62 Fig. 1|Permian|Permian|||||||
26193|Wagina Sandstone|22814|5|Briefly described|fig2|Permian|Permian|||||||
26193|Wagina Sandstone|22820|6|Mentioned|p22|||||||||
26193|Wagina Sandstone|23172|4|Described|Map Legend|Late Permian|Late Permian|||||||
26193|Wagina Sandstone|23174|4|Described|p15||Late Permian|||||||
26193|Wagina Sandstone|23279|4|Described|p15-7||Tatarian|(Clarke et al., 1951).||||||
26193|Wagina Sandstone|23761|5|Briefly described|p11|||||||||
26193|Wagina Sandstone|23762|5|Briefly described|Map Legend|Paleozoic|Paleozoic|||||||07-NOV-08
26193|Wagina Sandstone|23816|4|Described|p234, 235|Late Permian|Kungurian|Geological Province: Perth Basin. Underlying unit: Carynginia Formation (conformable). Max. thickness: 251 m.||||||
26193|Wagina Sandstone|24058|5|Briefly described|p111|Late Permian|Late Permian|Geological Basin: Perth Basin.||||||
26193|Wagina Sandstone|24160|6|Mentioned|p94|||Northern Perth Basin.||||||
26193|Wagina Sandstone|24410|6|Mentioned|p41|Permian|Permian|||||||
26193|Wagina Sandstone|24443|5|Briefly described|Fig.30|Early Triassic|Late Permian|Unconformably overlies Carynginia Formation. Conformably overlain by Kockatea Shale. Geological Province: Bight Basin.||||||10-JAN-05
26193|Wagina Sandstone|29633|6|Mentioned|p435|||Permian/Triassic boundary||||||
26193|Wagina Sandstone|29721|6|Mentioned|Table 226|||||||||
26193|Wagina Sandstone|30466|6|Mentioned|p7|||Upper Permian age||||||
26193|Wagina Sandstone|30545|6|Mentioned|Fig.2|||Lower Permian||||||
26193|Wagina Sandstone|30547|6|Mentioned|p426|||Correlation of Upper Permian and Lower Triassic.||||||11-APR-08
26193|Wagina Sandstone|30948|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26193|Wagina Sandstone|30973|6|Mentioned|Map legend|Kazanian|Kungurian|Kungurian ? - Kazanian||||||
26193|Wagina Sandstone|31394|6|Mentioned|p60|||See also P61,62. U.Permian||||||
26193|Wagina Sandstone|31561|6|Mentioned|p18|||See also map P20.||||||
26193|Wagina Sandstone|31562|6|Mentioned|p10|||Stratigraphic table||||||
26193|Wagina Sandstone|31568|5|Briefly described|p19|||Upper Permian.||||||05-MAR-08
26193|Wagina Sandstone|31617|6|Mentioned|p8|||||||||
26193|Wagina Sandstone|31910|4|Described|Table 1|||P18||||||
26193|Wagina Sandstone|32337|4|Described|p25|||||||||
26193|Wagina Sandstone|32642|6|Mentioned|p74|||Oil production||||||
26193|Wagina Sandstone|32648|6|Mentioned|p32|||Permian||||||
26193|Wagina Sandstone|32649|4|Described|p23|||See also Table 1||||||
26193|Wagina Sandstone|32712|6|Mentioned|Table 1|||||||||
26193|Wagina Sandstone|32714|6|Mentioned|Fig.2|||||||||
26193|Wagina Sandstone|32836|6|Mentioned|p5|||||||||
26193|Wagina Sandstone|32840|6|Mentioned|Table 1|||||||||
26193|Wagina Sandstone|33022|6|Mentioned|Fig.1|||||||||
26193|Wagina Sandstone|33052|6|Mentioned|Fig.1|||Kungurian & U.Perm.||||||
26193|Wagina Sandstone|33386|6|Mentioned|Fig.7|||||||||
26193|Wagina Sandstone|33701|6|Mentioned|Fig.1|||Artinskian.||||||
26193|Wagina Sandstone|34008|6|Mentioned|p77|||||||||
26193|Wagina Sandstone|34009|6|Mentioned|Table III|||||||||
26193|Wagina Sandstone|34138|6|Mentioned|Cor.Chart|||Kazanian||||||
26193|Wagina Sandstone|34532|6|Mentioned|Fig.2|||||||||
26193|Wagina Sandstone|34841|6|Mentioned|Fig.2|||||||||
26193|Wagina Sandstone|35282|6|Mentioned|Fig.2|||||||||
26193|Wagina Sandstone|35573|6|Mentioned|Fig.13|||Generalised stratigraphy - Perth Basin||||||
26193|Wagina Sandstone|35653|6|Mentioned|p1093|||Discussion of stratigraphy and basin development. See also Fig.3.||||||
26193|Wagina Sandstone|35873|6|Mentioned|p46|||||||||
26193|Wagina Sandstone|35901|6|Mentioned|p8|||||||||
26193|Wagina Sandstone|36100|6|Mentioned|Fig.2|||||||||
26193|Wagina Sandstone|36257|6|Mentioned|Table 2.1|||||||||
26193|Wagina Sandstone|36265|5|Briefly described|p134, Fig.3.26|Late Permian|Early Permian|Geological province: Perth Basin. Coal seams are lenticular.||||||04-MAR-08
26193|Wagina Sandstone|36266|5|Briefly described|p150|Permian|Permian|||||||31-MAR-08
26193|Wagina Sandstone|36293|2|Defined|p111|Late Permian|Late Permian|||||||
26193|Wagina Sandstone|36751|6|Mentioned|p179|||||||||
26193|Wagina Sandstone|36890|3|Fully described|p234|||Includes Indarra Beds||||||
26193|Wagina Sandstone|36899|6|Mentioned|Fig.3|||||||||
26193|Wagina Sandstone|36911|6|Mentioned|p57|||||||||
26193|Wagina Sandstone|37095|6|Mentioned|p247|||||||||
26193|Wagina Sandstone|37104|6|Mentioned|p271|||||||||
26193|Wagina Sandstone|37298|6|Mentioned|Fig.1|||||||||
26193|Wagina Sandstone|37577|6|Mentioned|p77|||||||||
26193|Wagina Sandstone|37812|6|Mentioned|p654|||||||||
26193|Wagina Sandstone|38352|6|Mentioned|p61|||||||||
26193|Wagina Sandstone|38484|6|Mentioned|p6|||||||||
26193|Wagina Sandstone|38486|6|Mentioned|p6|||||||||
26193|Wagina Sandstone|38655|6|Mentioned|p6|||||||||
26193|Wagina Sandstone|38998|6|Mentioned|p37|||||||||
26193|Wagina Sandstone|39854|6|Mentioned|p21|||||||||
26193|Wagina Sandstone|40306|6|Mentioned|p59|||||||||
26193|Wagina Sandstone|40340|6|Mentioned|p21|||||||||
26193|Wagina Sandstone|40346|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
26193|Wagina Sandstone|40347|5|Briefly described|p25|||||||||
26193|Wagina Sandstone|40794|5|Briefly described|Fig.3|||||||||
26193|Wagina Sandstone|40992|6|Mentioned|p6|||||||||
26193|Wagina Sandstone|41172|6|Mentioned|p123|||||||||
26193|Wagina Sandstone|41195|4|Described|p319|||||||||
26193|Wagina Sandstone|41474|6|Mentioned|p59|||||||||
26193|Wagina Sandstone|41589|5|Briefly described|p116|||||||||
26193|Wagina Sandstone|41728|6|Mentioned|p442|||||||||
26193|Wagina Sandstone|41729|6|Mentioned|p453|||||||||
26193|Wagina Sandstone|42075|5|Briefly described|Fig.7 P247|||||||||
26193|Wagina Sandstone|42309|6|Mentioned|p257|||||||||
26193|Wagina Sandstone|42641|6|Mentioned|p124|||Perth Basin||||||
26193|Wagina Sandstone|43015|5|Briefly described|Table 1,p319|||||||||
26193|Wagina Sandstone|43031|4|Described|p13,Fig.2|||||||||
26193|Wagina Sandstone|43067|5|Briefly described|p120,Fig.12,p124|||||||||
26193|Wagina Sandstone|43096|5|Briefly described|p7|||||||||
26193|Wagina Sandstone|43504|6|Mentioned|7|Late Permian|Early Permian|||||||
26193|Wagina Sandstone|44144|4|Described|p507 Tb.4-21, p509 Fig.4-145, p510|Late Permian|Kungurian|See also p511 Fig.4-147, p513, p523. Type Section: Irwin River, south branch; 28o59'30"S 115o35'00''E. 250m thick fluvial deposits. Reference Section: Woolaga Creek; 29o11'01"S, 115o40'00"E. A sandstone member in this unit is a gas reservoir.|||Yardarino Sandstone Member at top.|Overlies Carynginia Formation disconformably.|Fine- to medium-grained clayey quartz sandstone; minor conglomerate, shale, siltstone and coal.|
26193|Wagina Sandstone|44219|14|Not recorded|p31||Artinskian|||||||
26193|Wagina Sandstone|44994|6|Mentioned|Fig.7|||Correlation.||||||
26193|Wagina Sandstone|46849|6|Mentioned|Fig. 6|||||||||
26193|Wagina Sandstone|49644|5|Briefly described|Table|||||||||
26193|Wagina Sandstone|60384|6|Mentioned|p260 table 2|||Minor oil shows.  Fluorescence, cut, dead oil, trace oil, residual hydrocarbons.||||||
26193|Wagina Sandstone|61023|5|Briefly described|p20 Fig 10|Permian|Permian|Geological Province: Perth Basin.||||||05-MAR-08
26193|Wagina Sandstone|61811|4|Described|p3 Fig.2, pp32-33, p36, p39, p65.|Late Permian|Middle Permian|Northern Perth Basin. Lateral, fluvial equivalent of Dongara Sandstone and Beekeeper Formation to the south. Type section is in South Branch of the Irwin River near Wagina Well; further details in Appendix 1. The reference section extends east from Red Hill to the centre of a small syncline. Thickness to 250 m. Upper part also referred to as Yardarino Sandstone (Hosemann, 1971; Playford et al. 1976).||||Unconformably overlies Carynginia Formation.|White, cross-bedded, pebbly clayey sandstone, conglomerate, coal and a thin bed of carbonaceous shale.|
26193|Wagina Sandstone|62113|6|Mentioned|p620 Fig.3.|||Crops out on the Irwin Terrace, northern Perth Basin.||||||
26193|Wagina Sandstone|64580|4|Described|map legend||Late Permian|Fine- to medium-grained clayey quartz sandstone; minor conglomerate, shale, siltstone and coal.||||||09-DEC-08
26193|Wagina Sandstone|64635|5|Briefly described|p4 Fig.3, p16, p18, p22 Fig.20, p23   |Wuchiapingian|Kungurian|Of Clarke et al. (1951). North Perth Basin. Type and reference sections are detailed. Up to 250m thick. Palynological data indicate a Kungurian-Guadelupian age (Segroves, 1971; Kemp et al.,1977).||||Conformably or disconformably overlies the Carynginia Formation. Coeval with the Dongara Sandstone and Beekeeper Formation.|Consists chiefly of fine- to medium-grained cross-bedded clayey sandstone with lesser amounts of conglomerate, siltstone, shale and coal.|
26193|Wagina Sandstone|64972|6|Mentioned|p617 Fig. 5|Late Permian|Late Permian|Geological Province: Perth Basin.||||||
26193|Wagina Sandstone|64974|6|Mentioned|p144 Fig. 3|Tatarian|Ufimian|Geological Province: Perth Basin.||||||24-JUN-09
26193|Wagina Sandstone|64980|5|Briefly described|pp625-634.|||Perth Basin. Hydrocarbon reservoir; its properties and field history are detailed in the article.|||||Fine to coarse, moderately to poorly sorted, quartzose sandstone with shale intercalations.|
26193|Wagina Sandstone|67135|5|Briefly described|p5 Fig.7.|Permian|Permian|North Perth Basin. Lateral equivalent of Dongara Sandstone to the south.||||Is overlain by Kockatea Shale.||
26193|Wagina Sandstone|67340|6|Mentioned|p6, 8, 25|Permian|Permian|Northern Perth Basin. Thermal rock properties.||||||
26193|Wagina Sandstone|67370|6|Mentioned|p328.|Late Permian|Late Permian|Cool but not cold depositional environment.||||||
26193|Wagina Sandstone|67925|5|Briefly described|Ch2 p11, Ch4 p8 fig 2|Upper Permian|Upper Permian|Northern and Central Perth Basin. Age equivalent of the Willespie Formation.||||Unconformably overlies the Carynginia Formation.||
26193|Wagina Sandstone|69029|6|Mentioned|p332|Permian|Permian|Of Perth Basin.||||Overlain by Dongara Sandstone. Underlain by Willespie Formation.||
26193|Wagina Sandstone|69081|6|Mentioned|p735|Permian|Permian|oil and gas produced. Age: upper Permian. Geol. Prov: Perth Basin||||||
26193|Wagina Sandstone|69182|5|Briefly described|Ch2 p3, Ch2 p9, Ch2 p11, Ch2 p12|Middle Permian|Middle Permian|Perth Basin. Deposited in a fluvial to shallow marine environment. Potentially significant reservoir for the storage of carbon dioxide as its porosity is generally between 10 and 25 percent and permeability is often in the hundreds of mD. See also Ch2 p34-p41, Ch2, p44-p49, Ch2 p54-p55, Ch2 p57, Ch2 p60, Ch2 p64-p66, Ch2 p80, Ch2 p83-p84, Ch2 p89-p92, Ch2 p94-p96, Ch2 p98-p102, Ch2 p104, Ch2 p106, Ch2 p108, Ch2 p110-p112. ||||Unconformably overlain by the Kockatea Shale. Conformably overlies the Carynginia Formation. Equivalent to the Beekeeper Formation and the Dongara Sandstone.|Fine-grained, well-sorted sandstones.|
26193|Wagina Sandstone|70097|5|Briefly described|p2, p9, p20 Fig.4|Wuchiapingian||In Fig.4: age range for undifferentiated Dongara and Wagina Sandstones at Greenough/Bookara Shelf and Dongara Saddle is Wordian - late Wuchiapingian; in Irwin Terrace, Capitanian - Wuchiapingian; and, in Dandaragan Trough, Wordian. Crostella, 1995; Mory and Iasky, 1996. See also Wagina Formation in this paper.||||Overlies Carynginia Formation. Is overlain by Dongara, Wittecarra or Victoria Plateau Sandstones.|A series of coalesced, coarse-grained alluvial deltas.|12-SEP-17
26193|Wagina Sandstone|70128|5|Briefly described|p449|Permian|Permian|Northern Perth Basin.||||Conformably overlies Carynginia Formation. Is overlain unconformably by Kockatea Shale.||
26193|Wagina Sandstone|70774|5|Briefly described|p5 fig 3|Dorashamian|Kazanian|Northern Perth Basin.||||Equivalent to the Dongara Sandstone and the Beekeeper Formation.||
26193|Wagina Sandstone|70796|5|Briefly described|500k_interpgeop14_lut.csv|Lopingian|Lopingian|Perth Basin. Formed during Gondwana breakup along the western margin.|ca 270 to 252.17 Ma (biostrat)||||Fine to mediumgrained, clayey quartz sandstone; minor conglomerate, shale, siltstone and coal|
26193|Wagina Sandstone|70826|6|Mentioned|p6 tbl 3|Permian|Permian|Perth Basin.||||||
26193|Wagina Sandstone|71146|6|Mentioned|p6|Lopingian|Guadalupian|Perth Basin.||||||
26193|Wagina Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, shale, siltstone, sandstone|
26193|Wagina Sandstone|71269|5|Briefly described|GEOL_LUT_CSV files|Lopingian|Guadalupian|Of Perth Basin. Events: Mid-Miocene transgression, 15 Ma (15-15 Ma); Wilson Bluff transgression, 42 Ma (42-42 Ma); Kings Park transgression, 56 Ma (56-56 Ma); Gondwana breakup-western margin (210-125 Ma); Jurassic-Early Cretaceous rifting, Perth Basin (168-133 Ma);??. See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv.|270-252.17 Ma (biostrat)||||Fine- to medium-grained, clayey quartz sandstone; minor conglomerate, shale, siltstone and coal|
26193|Wagina Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Lopingian|Guadalupian|Perth Basin.  Age from biostratigraphy.||Permian package 3, Perth Basin. |||Fine- to medium-grained, clayey quartz sandstone; minor conglomerate, shale, siltstone and coal.|
26193|Wagina Sandstone|72258|5|Briefly described|p129,133,135|Lopingian|Guadalupian|Of Perth Basin. Neoarchean (2800-2600 Ma) detrital zircons attributed to Yilgarn Craton, along eastern boundary of Perth Basin (Kositcin et al., 2008; Mole et al., 2013; Nemchin and Pidgeon, 1997). Older material (3700-3000 Ma) probably also derived from Yilgarn Craton. Major peak in Mesoproterozoic (1300-1100 Ma) and minor Late Paleoproterozoic (1800-1600 Ma) detrital zircons correlate with characteristic ages and Hf isotopic signatures of magmatism in the Albany-Fraser-Wilkes Orogen (Clark et al., 2000; Fitzsimons, 2000, 2003; Kirkland et al., 2011; Spaggiari et al., 2015). Late Meso- to Early Neoproterozoic (1100-900 Ma) detrital zircons atributed to Pinjarra Orogen. Bimodal Neoproterozoic 750 and 500 Ma peaks in detrital zircon ages also likely to be derived locally from Pinjarra Orogen (p134-135 describes potential, but unlikely Gondwanan sources).||||Laterally gradees into Willespie Formation.||
26193|Wagina Sandstone|72505|5|Briefly described|p890|Changhsignian|Wuchiapingian|Perth Basin. Correlates with the Dulhuntyispora parvithola zone.||||Interfingers with the Dongara Sandstone. Overlain by the Kockatea Shale.||
26193|Wagina Sandstone|72910|6|Mentioned|p4 Fig.3.|Late Permian|Late Permian|Shown as part of the Northern Perth Basin.||||Underlies the Kockatea Shale and shown as being laterally equivalent to Dongara Sandstone.||
26193|Wagina Sandstone|73513|5|Briefly described|p30 Fig.2, p32-33|Tatarian|Kazanian|Perth Basin. Deposited in shoreface settings.||||Overlies Carynginia Formation, underlies Dongara Sandstone|Sandstone.|
26193|Wagina Sandstone|73623|5|Briefly described|p4|Guadalupian|Guadalupian|Irwin Basin.||||Overlies Carynginia Formation. Correlative of Kennedy Group.||
35794|Wahlgu Formation|23571|4|Described|p7, 10, 11|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin. Underlying Unit: Steptoe Formation (unconformable). Overlying Unit: Table Hill Volcanics (unconformable). Max. thickness: >500m||||||
35794|Wahlgu Formation|24161|4|Described|p9 Fig.6, p14|Early Cambrian|Neoproterozoic|Proposed to replace the Lupton Formation for the Supersequence 3 glacial deposits. Unconformably overlies the Steptoe and Kanpa Formations. Overlain by the McFadden Formation equivalent. Average Thickness: 300m. Geological Province: Officer Basin.||||||
35794|Wahlgu Formation|24390|5|Briefly described|p11 Fig. 6|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
35794|Wahlgu Formation|50085|5|Briefly described|p11 Fig. 6|Neoproterozoic|Neoproterozoic|Age: ~600Ma.  Geological Province: Officer Basin.||||||
35794|Wahlgu Formation|50205|5|Briefly described|p59 Fig.1|Neoproterozoic|Neoproterozoic|Of Officer Basin.|620-580 Ma|||||
35794|Wahlgu Formation|61023|5|Briefly described|p15 Fig. 8|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||11-APR-08
35794|Wahlgu Formation|61732|3|Fully described|p4 Fig. 3, p86|Marinoan|Marinoan|Of Buldya Gp. Sandstone, mudstone, diamictite and carbonate. Unconformably overlain by Table Hill Volcanics. Disconformable on Steptoe Formation. Geol.Prov: central and southern Officer Basin. See also p58 Fig. 22.||||||07-FEB-11
35794|Wahlgu Formation|62453|3|Fully described|p42|Ediacaran|Cryogenian|Parts previously assigned to Lupton Formation. Geological Province: Officer Basin. Underlies: Lungkarta Formation. Overlies disconformably: Steptoe Formation. Diamictite, mudstone, sandstone, conglomerate.||||||
35794|Wahlgu Formation|62987|5|Briefly described|p30, p31|Neoproterozoic|Neoproterozoic|Previously assigned to the Lupton Formation. Overlies the Buldya Group; overlain by Lungkarta Formation. Geological Province: Officer Basin. Correlates with the Marinoan glaciation.||||||24-SEP-08
35794|Wahlgu Formation|63022|5|Briefly described|p1014, p1015|||Disconformably overlies Buldya Group. Geological Province: Officer Basin. Glacial deposits - part of the Marinoan glacial succession. Supersequence 3.||||||10-AUG-07
35794|Wahlgu Formation|64103|4|Described|p399 Fig. 2, p400, p400 Fig. 3, p402|Ediacaran|Ediacaran|Formation is Fm in text. Geological Province: Officer Basin. Depositional environment in present study is glacigene, predominantly fluvioglacial. See p401-402 for detailed information. Glacially related diamictite, conglomerate, mudstone and sandstone.||||||03-SEP-14
35794|Wahlgu Formation|64325|5|Briefly described|p82 Fig. 2, p85|Neoproterozoic|Neoproterozoic|A unit of Supersequence 3. Geological Province: western Officer Basin. Diamictite unit representative of Marinoan glaciation of Offcier Basin.||||||26-AUG-08
35794|Wahlgu Formation|65363|4|Described|pp1-2, p6 Fig.5, pp7-8. |Neoproterozoic|Neoproterozoic|Officer Basin. Porosity and permeability are briefly discussed. Hydrocarbon traces were found to be almost entirely due to carbonate cements. Mafic igneous rock clasts are relatively fresh. Some sandstones contain green clay pellets, possibly galuconite. This suggests cold climate, at least periodic marine influence; the sediment appears to have been dumped by retreating ice sheets. Correlated with Marinoan glacial succession throughout the Centralian Superbasin and Adelaide Rift Complex; and with Boondawari Formation. Excellent reservoir quality in the upper part.|c.610 - 590 Ma.|||Disconformably overlies Kanpa Formation. Is overlain by Lungkarta Formation.|Reddish-brown, sometimes grey, poorly sorted, massive diamictites with mudstone or sandy mudstone matrix and scattered granule to boulder clasts, some with facets and striations; mudstone, multicoloured sandstone.|
35794|Wahlgu Formation|65364|5|Briefly described|p81|||Officer Basin.||||Overlain by Lungkarta Formation, underlain by Kanpa Formation.|Red diamictite and mudstone, multicoloured sandstone.|16-MAR-12
35794|Wahlgu Formation|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Cryogenian|Central Officer Basin. Includes stromatolite assemblage.||||||
35794|Wahlgu Formation|65366|6|Mentioned|p19, 23 Fig. 3, p24|Neoproterozoic|Neoproterozoic|Central Officer Basin. Diamictite. ?Cryogenian||||||19-MAR-12
35794|Wahlgu Formation|65368|5|Briefly described|p12, p14 Fig. 1, p16 Fig. 2|Neoproterozoic|Neoproterozoic|Diamictite and mudstone.||||||19-MAR-12
35794|Wahlgu Formation|65370|5|Briefly described|p39, 39 Tb. 1|||In Lancer 1: red-brown medium to coarse grained sandstone.||||||04-MAY-11
35794|Wahlgu Formation|65371|5|Briefly described|p53, 54 Fig. 1, p55-57, p58|||Officer Basin. Disconformable on Kanpa Formation, Buldya Group. Disconformably overlain by Lungkarta Formation. Diamictite, mudstone, multicoloured sandstones.  Glacial, and 'uncertain but aquatic' depositional environments. Mineralogy discussed.||||||
35794|Wahlgu Formation|67195|4|Described|p10 fig 6, p19 table 1, p44, 47 |Neoproterozoic|Neoproterozoic|Western Officer Basin. Thermal conductivity of 2.69 W/mK. See also App 1, App 2.|||||Diamictite; red medium grained sandstone with occasional granule-small pebble float; siltstone; red claystone; dark brown claystone.|
35794|Wahlgu Formation|67200|5|Briefly described|app 2 p9||||||||Claystone and medium grained sandstone.|
35794|Wahlgu Formation|67454|4|Described|p563, pp564-566, pp568-570.|Neoproterozoic|Neoproterozoic|Officer Basin. The age is predicated on correlation with Marinoan glacial successions elsewhere in Australia, eg Elatina Formation of the Adelaide Rift Complex. Palaeomagnetic results from the Lancer 1 drillhole are detailed and discussed. The combination of low palaeolatitude and glacial strata remains enigmatic.|c.600 Ma.|||Overlies Buldya Group disconformably. Is overlain by Lungkarta Formation.|Predominantly glacial diamictite; basal well-sorted sandstone, mudstone and conglomerate.|
35794|Wahlgu Formation|68270|4|Described|p678,682-684,686-687|Cryogenian|Cryogenian|Western Officer Basin. Type section occurs in Empress 1/1A, lat. 27'03'13"S, long. 125'09'24"E.  Known only from drillholes. Between 122 (Lancer-1)  and 479m (Vines-1) thick. Fluvio-glacial to glacio-marine deposit.  Contains columnar stromatolite Anabaria = Kotuikania juvensis (Elleria minuta) in diamictite, and could be used a straitgraphic marker in central Austtralian basins. Related to Elatina glaciation. Correlative to Elatine Formation and equivalents. Laterally equivalent to the lower Boondawari Formation.||||Overlain disconformably by Lungkarta Formation. Underlain disconformably by Steptoe Formation (karstified surface), and Pirrilyungka Formation.|Sandy diamictite; minor mudstone, sandstone, conglomerate and dolomite, including uppermost 1.5 m in Empress 1/1A that resembles upper marker cap dolomite in the Amadeus Basin.|03-JUL-19
35794|Wahlgu Formation|68277|5|Briefly described|p96, 103|Neoproterozoic|Neoproterozoic|Officer Basin.||||Correlated with Elatina Formation (SA). Possible correlative of Chambers Bluff Tillite (SA).|Contains a diamictite level.|
35794|Wahlgu Formation|69003|6|Mentioned|p4, p60|||Paterson Orogen.||||||
35794|Wahlgu Formation|69029|6|Mentioned|p329|Neoproterozoic|Neoproterozoic|Of Officer Basin.||||Overlain unconformably by McFadden Formation or Vines Formation. Underlain unconformably by Steptoe Formation.||
35794|Wahlgu Formation|69091|5|Briefly described|p30 Fig.3.5, p38 Fig.3.7, see comments|Neoproterozoic|Neoproterozoic|Crops out in northwest Officer Basin. Deposited during Elatina glaciation. See also p41 Fig.3.8, p43, p44, p81 Fig.4.17, p174 Fig.9.5, p177 Fig.9.6, p200 Fig.10.2.||||Overlies Pirrilyungku Formation; is disconformably overlain by Table Hill Volcanics.|Brownish to varicoloured and polymictic diamictite.|07-OCT-14
35794|Wahlgu Formation|69445|6|Mentioned|p30:5, 17|||Officer Basin.||||Is overlain conformably by Table Hill Volcanics.||12-JUL-16
35794|Wahlgu Formation|70793|4|Described|500k_interpgeop14_lut.csv|Cryogenian|Cryogenian|Of Officer Basin (Phase 1), Centralian Superbasin. Events: Officer Basin Cenozoic diapirism (66-0.01 Ma); Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 500k_interpgeop14_lut.csv, 2_5m_interpgeop15_lut.csv.|850-635 Ma (biostrat)||||Sandstone, diamictite (commonly polymictic), siltstone, dolomite; characteristically reddish|
35794|Wahlgu Formation|70826|6|Mentioned|p5 tbl 2|||Supersequence 3, Centralian Superbasin.||||||20-APR-20
35794|Wahlgu Formation|71268|4|Described|GEOL_LUT_CSV files|Cryogenian|Cryogenian|Of Officer Basin (Phase 2). Events: Officer Basin Cenozoic diapirism (66-0.01 Ma); Delamerian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|720-635 Ma (inferred)||||Sandstone, diamictite (commonly polymictic), siltstone, and dolomite; characteristically reddish|
35794|Wahlgu Formation|71800|6|Mentioned|p26-p27|Ediacaran|Ediacaran|Officer Basin.||||Overlain by the McFadden Formation and the Hussar Formation.|Coarse sandstone.|
35794|Wahlgu Formation|72034|5|Briefly described|500k_interpgeop16_lut|Cryogenian|Cryogenian|Officer Basin (Phase 1).|||||Sandstone, diamictite (commonly polymictic), siltstone, dolomite; characteristically reddish.|
35794|Wahlgu Formation|73392|6|Mentioned|p4||||||||Sampled from core of GSWA Vines 1 well.|
75709|Waladah Gabbro|66195|4|Described|p602 Fig.4, p605, p608-9, p611 Fig.9|Neoarchean|Neoarchean|Of Yalgowra Suite. Age: 2711 +/- 2 Ma. Gabbronorite, gabbro, leucocratic anorthosite. Up to 2 km thick. See also sample 185927 p607.||||||13-MAR-12
75709|Waladah Gabbro|67129|5|Briefly described|p54-55|Archean|Archean|Murchison Domain, Youanmi Terrane.|2711 +/- 2 Ma.|Yalgowra Suite.|||Gabbro, gabbronorite.|
75709|Waladah Gabbro|68561|4|Described|GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. Mafic sill.  U-Pb zircon age: 2711 +/- 2 Ma interpreted as the igneous crystallization age of the gabbro sill. Relationships, age from Geochron file 185927.1.pdf.||Yalgowra Suite|||Includes very coarse grained to pegmatoidal leucogabbro|
75709|Waladah Gabbro|68698|5|Briefly described|p8||||2711 +/- 2 Ma (Wingate et al., 2010).|Yalgowra Suite.|||Includes leucogabbro sills.|
75709|Waladah Gabbro|70796|6|Mentioned|185927.1.pdf|||Murchison Domain.||Yalgowra Suite||||
75709|Waladah Gabbro|70830|5|Briefly described|p27-p28|||Youanmi Terrane. ||||||
75709|Waladah Gabbro|71168|5|Briefly described|p7|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Yalgowra Suite||||
75709|Waladah Gabbro|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Sample GSWA 185927 (leucogabbro sill) yielded a weighted mean 207Pb/206Pb date of 2711+\-2 Ma, interpreted as the igneous crystallization age of the gabbro sill. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv.|2711+\-2 Ma|Unit of Yalgowra Suite.|||Gabbro with gabbronorite base and harrisitic leucogabbro top contact; metamorphosed|
75709|Waladah Gabbro|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|c.2711 Ma.|Yalgowra Suite.|||Gabbro with gabbronorite base and harrisitic leucogabbro top contact, metamorphosed; (separately mapped) metamorphosed leucogabbro and metamorphosed gabbronorite.|
75709|Waladah Gabbro|73596|6|Mentioned|p1165|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane.|2711 +/- 2 Ma.|Yalgowra Suite.||||
26978|Walatharra Formation|23815|6|Mentioned|p305|Pleistocene|Pleistocene|Geological Province: Carnarvon Basin.||||||
26978|Walatharra Formation|36890|6|Mentioned|p305|||||||||
26978|Walatharra Formation|37016|6|Mentioned|Map legend|Quaternary|Pliocene|Quaternary to Pliocene||||||
26978|Walatharra Formation|39427|4|Described|Table 1|||||||||
26978|Walatharra Formation|41271|4|Described|p198|||||||||
26286|Walcott Formation|6876|6|Mentioned|p100 Fig.5.|Paleogene|Paleogene|The 'Formation' was left off the diagram due to space constraints.||||||
26286|Walcott Formation|23726|5|Briefly described|p8 Fig 2c|Eocene|Eocene|Underlying unit Wilcox Formation. Geological Province: Carnarvon Basin.||||||
26286|Walcott Formation|40617|5|Briefly described|p16|||||||||
26286|Walcott Formation|40800|2|Defined|p22|middle Eocene|middle Eocene|||||||
26286|Walcott Formation|41271|3|Fully described|p171|||||||||
26286|Walcott Formation|41437|5|Briefly described|p70|||||||||
26286|Walcott Formation|41438|5|Briefly described|p110|||||||||
26286|Walcott Formation|41732|6|Mentioned|Fig.3|||||||||
26286|Walcott Formation|42116|5|Briefly described|Fig.1 P6|||||||||
26286|Walcott Formation|43712|6|Mentioned|Fig.10,p52||Eocene|||||||
26286|Walcott Formation|43724|6|Mentioned|Fig.15,p65||Eocene|||||||
26286|Walcott Formation|61155|5|Briefly described|p15|Late Eocene|Middle Eocene|47.5-37.5Ma. Max. thickness: 400m. Geological Province: Carnarvon Basin /offshore.||||||
26286|Walcott Formation|62734|5|Briefly described|p1362 Fig. 2|Eocene|Eocene|Geological Province: Barrow Sub-basin.||||||01-SEP-08
26286|Walcott Formation|62837|5|Briefly described|Stratigraphic columns|Eocene|Eocene|Age: 50-35Ma. Geological Province: Dampier Sub-basin, Rankin Platform and Beagle Sub-basin.||||||
26286|Walcott Formation|67200|5|Briefly described|p8 fig 6, |Eocene|Eocene||||||laminated marl.|
26286|Walcott Formation|67970|6|Mentioned|p25 Fig.4.|Priabonian|Lutetian|Exmouth Plateau.||||||
26286|Walcott Formation|69692|6|Mentioned|p4|Eocene|Eocene|Northern Carnarvon Basin.||||Overlies Wilcox Formation. Is overlain by Cape Range Group.||
26286|Walcott Formation|70066|5|Briefly described|Dampier: Fig.2. Exmouth: Fig.2|Priabonian|Lutetian|See also Regional: Fig.6. Northern Carnarvon Basin.||||Overlies Wilcox Formation. Is overlain by Mandu Limestone.||
26286|Walcott Formation|70906|5|Briefly described|p757-758|Oligocene|Eocene|Gorgon Platform.||||Overlies Wilcox Formation. Is overlain by Tealla Limestone.||
79111|Waldburg Dolerite|70019|6|Mentioned|p93-94|Calymmian|Calymmian|Geological province: Gascoyne Province, Capricorn Orogen. Intrusion within the lower Edmund Group/Irregully Formation.|1515-1500 Ma|||||
79111|Waldburg Dolerite|70795|5|Briefly described|100k_geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Also 2_5m_interpgeop15_lut.csv, 100k_interpgeop_lut.csv, 206991.1.pdf, West Australian Craton, Edmund Basin|1517-1500 Ma|Edmund Group||Intrudes Edmund Group, Irregully Formation, Yilgatherra Formation, Kiangi Creek Formation|Dolerite and gabbro sills.|
79111|Waldburg Dolerite|70814|5|Briefly described|p3, p5, p8, p12, p22|Calymmian|Calymmian|Edmund Basin. Ages are of igneous crystallization from Wingate et al., 2015a and 2015b. Another age of 1513 +/- 4 Ma is given in Wingate et al., 2013a and an age of 1505 +/- 3 Ma (Wingate et al., 2012b).|1517-1505 Ma|||Intrudes the Kiangi Creek Formation and the Yilgatherra and Irregully Formations of the Edmund Group.||
79111|Waldburg Dolerite|70826|6|Mentioned|p10|Mesoproterozoic|Mesoproterozoic|Actually listed as Waldburg Dolerite Suite, along with Narimbunna Dolerite Suite.||||Intrudes the Edmund Group. Broadly coeval with Warlawurru Supersuite in Musgrave province.||20-MAY-20
79111|Waldburg Dolerite|71869|6|Mentioned|p4||||c. 1500 Ma|||||
79111|Waldburg Dolerite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Edmund Basin. |Max age 1517+/-8 Ma, min 1505+/-3 Ma.|||Intruded into Edmund Group.|Dolerite and gabbro sills intruded into Edmund Group.|
79111|Waldburg Dolerite|73102|5|Briefly described|p2-3, p6-7, p12, p17-19, 28|Calymmian|Calymmian|Gascoyne Province. Intrudes sedimentary rocks of the Edmund Basin, but not Collier Basin.|1514-1505 Ma|||Intruded by Mundine Well Dolerite. Intrudes lower part of Edmund Group.|Dolerite and gabbro sills intruded into lower part of Edmund Group.|
79111|Waldburg Dolerite|73442|4|Described|p1-14, p16 Fig.15, p19, p23-27, p35-38|Calymmian|Calymmian|Capricorn Orogen, western. Ages inclue three samples with a mean age of 1514+/-3 Ma, and a U-Pb zircon age of 1517+/-8 Ma (Wingate et al., 2015a). Mainly NW-striking, emplaced only within the Edmund Basin in a structural corridor between the Lyons River Fault and Ti Tree Shear Zone. Intrudes middle and lower strata of the Edmund Group - Depositional Packages 1 to 3 (Thorne, 2015a-c). The sills appear laterally continuous (up to 36km long), thickness ranges from 100-500m. Characterised as high-Fe tholeiites. Distinctive geochemical characteristics include low concentrations of most REE and HFSE, and weakly fractionated REE. Location in text includes iii-iv, p15 Fig.13-14, p41.|1514-1505 Ma, 1517+/-8 Ma U-Pb zircon, baddeleyite|||Intruded into Edmund Group, lower part|Comprises four, mainly medium- to coarse-grained tholeiitic dolerite sills containing patches of very coarse-grained dolerite to leucogabbro, and rare felsic veins. Typically altered, strongly fractured, exhibits spheroidal weathering.|
74845|Walganna Suite|64891|5|Briefly described|p37 Fig. 2, p42, p52-53 Tb. 1|Archean|Archean|Of Bald Rock Supersuite. Includes Garden Rock, Telegootherra + Taincrow Monzogranites. In Murchison Domain. Age: 2637-2602Ma. Biotite(-muscovite) monzogranites to syenogranites. Referred to as a Granite Suite in Fig. 2||||||07-FEB-11
74845|Walganna Suite|65546|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Yilgarn Craton. 2637-2602 Ma. Of Bald Rock Supersuite. Granites and undivided metamorphics.||||||
74845|Walganna Suite|65548|5|Briefly described|Map Legend|Neoarchean|Neoarchean|2637-2602 Ma. Of Bald Rock Supersuite, Yilgarn Craton. Includes granites and undivided metamorphics.||||||
74845|Walganna Suite|65550|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Bald Rock Supersuite. Age of 2637-2602 Ma given. Granite, undivided with local biotite- or amphibole-rich bands; metamorphosed; includes deeply weathered rock.||||||
74845|Walganna Suite|66195|5|Briefly described|p599 Fig.2|Neoarchean||In the Bald Rock Supersuite. Granitic.||||||13-MAR-12
74845|Walganna Suite|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Mapped as five separate units, only two of which - Telegootherra and Garden Rock Monzogranites - are named.||Unit in Bald Rock Supersuite.|Includes Telegootherra Monzogranite and Garden Rock Monzogranite, and three separately-mapped but un-named units.|||
74845|Walganna Suite|67129|6|Mentioned|p18 Fig.19, p47, p57|Archean|Archean|Murchison Domain, Youanmi Terrane. Named after Walganna (Walgahna) Rock, the type area for the Suite, famous for Aboriginal rock art.|2640-2600 Ma|Bald Rock Supersuite|||Post-tectonic granites; includes coarse K-feldspar-porphyritic monzogranite.|07-SEP-17
74845|Walganna Suite|68519|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|2640-2600 Ma|Of the Bald Rock Supersuite.|||Monzogranite; pegmatite with granophyric intergrowths; muscovite-rich pegmatite with books of muscovite and quartz-feldspar intergrowths greater than 1 cm; all metamorphosed.|
74845|Walganna Suite|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. Age: 2637 - 2602 Ma, from geochron file 178197.1.pdf.||Bald Rock Supersuite|Includes Cootharra Monzogranite, Garden Rock Monzogranite, Telegootherra Monzogranite, Yarrabubba Monzogranite and 4 unnamed units.||Monzogranite, monzogranite to syenogranite, granite, hornblende syenite|
74845|Walganna Suite|68698|5|Briefly described|p4-6, p8, p10, p14-17, p27-28|Neoarchean|Neoarchean|Post-tectonic, undeformed granites. A sample of biotite monzogranite has a magmatic crystallisation age of 2623 +/- 9 Ma (Wingate et al., 2009). Geochemistry is discussed. REE plots.|c.2630-2610 Ma.|Bald Rock Supersuite.|||Biotite +/- muscovite monzogranite to syenogranite that ranges from coarsely K-feldspar-porphyritic to coarse-grained and equigranular.|
74845|Walganna Suite|69014|6|Mentioned|Map Legend|Neoarchean|Neoarchean|Murchison Domain. Also includes 4 unnamed facies, mapped separately.|2640-2600 Ma|Of the Bald Rock Supersuite.|Includes Cootharra Monzogranite and Garden Rock Monzogranite.||Includes undeformed monzogranite to syenogranite; megacrystic monzogranite intruded by fine-grained monzogranite; equigranular monzogranite; undeformed medium- to coarse-grained monzogranite.|01-MAY-14
74845|Walganna Suite|69583|4|Described|p49, p51, p99, p126, p130; Plates 2, 3|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Seismic interpretation. Non-reflective; has a flat-lying fabric; forms a sheet-like intrusion.|2640-2601 Ma.|Bald Rock Supersuite.|Telegootherra, Garden Rock, Taincrow Monzogranites.|Intrudes Windimurra Igneous Complex.|Biotite +/- muscovite monzogranite to syenogranite that ranges from coarsely K-feldspar porphyritic to coarse-grained and equigranular.|
74845|Walganna Suite|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean|||Bald Rock Supersuite|Telegootherra Monzogranite, Garden Rock Monzogranite, Taincrow Monzogranite|||
74845|Walganna Suite|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.|||Telegootherra, Garden Rock, Taincrow Monzogranites.|||
74845|Walganna Suite|69626|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton|2630-2600 Ma|Bald Rock Supersuite|||Monzogranite, locally rich in muscovite and biotite; predominantly with equigranular texture and locally K-feldspar porphyritic; metamorphosed.|
74845|Walganna Suite|69627|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton||Bald Rock Supersuite|Garden Rock Monzogranite, Telegootherra Monzogranite|||
74845|Walganna Suite|69628|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton|2630-2600 Ma|Bald Rock Supersuite|Cootharra Monzogranite, Yarrabubba Monzogranite||Monzogranites.|
74845|Walganna Suite|70020|5|Briefly described|p118|Neoarchean|Neoarchean|Geological province: Yilgarn Craton.||Unit of Bald Rock Supersuite.||Overlain by Wogala Suite. Underalin by Jungar Suite.||
74845|Walganna Suite|70030|5|Briefly described|p192|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton.||Unit of Bald Rock Supersuite.||||
74845|Walganna Suite|70139|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton. Three un-named facies are mapped separately.||Bald Rock Supersuite.|Garden Rock, Cootharra Monzogranites.||Undeformed, metamorphosed monzogranite to syenogranite.|
74845|Walganna Suite|70140|5|Briefly described|Map legend.|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. 7 un-named facies are mapped separately.||Bald Rock Supersuite.|Walgoo Monzogranite.||Pegmatites, muscovite-rich or with granophyric intergrowths; monzogranites: K-feldspar megacrystic, muscovite and/or biotite rich or with abundant rafts of metasedimentary rock; metamorphosed granitic rock with abundant pegmatite veins.|
74845|Walganna Suite|70153|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean||2647 - 2600 Ma (inferred).|Bald Rock Supersuite|||Monzogranite, locally rich in muscovite and biotite; predominantly with equigranular texture and locally K-feldspar porphyritic; includes deeply weathered rock.|
74845|Walganna Suite|70156|4|Described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma).|2647-2600 Ma (inferred)|Unit of Bald Rock Supersuite.|||Monzogranite, locally rich in muscovite and biotite; predominantly with equigranular texture and locally K-feldspar porphyritic; includes deeply weathered rock|
74845|Walganna Suite|70226|5|Briefly described|Map legend.|Neoarchean|Neoarchean|Also misspelt as Walganna Supersuite on main map legend. Yilgarn Craton.|c. 2626 Ma (Fletcher and McNaughton, 2002).|Bald Rock Supersuite|Wangata Monzogranite||Monzogranites; minor pegmatite.|16-DEC-15
74845|Walganna Suite|70419|5|Briefly described|p12, p19, p25|||Density is 2.65 g/cm3. Inferred to intrude the base of the Windimurra Igneous Complex.|||||Post-tectonic granitic rocks; includes monzogranite.|
74845|Walganna Suite|70769|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton. The two facies are mapped separately.|2647-2600 Ma.|Bald Rock Supersuite.|||K-feldspar-porphyritic to megacrystic monzogranite; locally with biotite up to 10%. Equigranular monzogranite with 4-10mm grain size.|03-MAR-17
74845|Walganna Suite|70770|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton.|2647-2600 Ma.|Bald Rock Supersuite.|Walgoo Monzogranite.|||
74845|Walganna Suite|70794|4|Described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton. Also 2_5m_interpgeop15_lut.csv.|2647-2600 Ma inferred|Bald Rock Supersuite|||Monzogranite, locally rich in muscovite and biotite; predominantly with equigranular texture and locally K-feldspar porphyritic. Syenogranite.|
74845|Walganna Suite|70795|5|Briefly described|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean||2647-2600 Ma||||Monzogranite to syenogranite; undeformed.|
74845|Walganna Suite|70796|4|Described|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton. See also 100k_geologyl_lut.csv, 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 155513.1.pdf, 178197.1.pdf, 185929.1.pdf, 198213.1.pdf, 207630.1.pdf, Austin100_2442_stratig.pdf, Badja100_2240_stratig.pdf, Bungar100_2539_stratig.pdf, Coolamaninu100_2540_stratig.pdf, Cue100_2443_stratig.pdf, Koonmarra100_2445_stratig.pdf, Madoonga100_2444_stratig.pdf, Nowthanna100_2643_stratig.pdf, Reedy100_2543_stratig.pdf, Tieraco100_2545_stratig.pdf, Windimurra100_2641_stratig.pdf, Wynyangoo100_2542_stratig.pdf, Yalgoo100_2241_stratig.pdf, Youanmi100_2640_stratig.pdf.|ca 2647 to 2600 Ma (inferred)|Bald Rock Supersuite|Includes the Telegootherra Monzogranite, Wangata Monzogranite, Cootherra Monzogranite, Garden Rock Monzogranite, Walgoo Monzogranite, Yarrabubba Monzogranite.|Intruded by the Marlolmumbah Granite.|Monzogranite to syenogranite; undeformed; Muscoviterich pegmatite; Pegmatite with granophyric intergrowths; Monzogranite, locally rich in muscovite and biotite; predominantly with equigranular texture and locally Kfeldspar porphyritic.|
74845|Walganna Suite|70826|6|Mentioned|p9|Neoarchean|Neoarchean||||||Granites.|
74845|Walganna Suite|70830|5|Briefly described|p9|||Murchison Domain.||Bald Rock Supersuite||||
74845|Walganna Suite|71159|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton. The two facies are mapped separately.||Bald Rock Supersuite.|Cootharra Monzogranite.||K-feldspar-porphyritic to megacrystic monzogranite; medium- to coarse-grained equigranular monzogranite; undeformed monzogranite; undeformed muscovite monzogranite.|
74845|Walganna Suite|71168|5|Briefly described|p7|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c. 2630-2610 Ma|Bald Rock Supersuite|||Granitic rocks.|
74845|Walganna Suite|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma). Monzogranites are essentially undeformed, except for localised, E-trending brittle shear zones spatially associated with E-trending Proterozoic dolerite dykes. Commonly contains older xenoliths (Van Kranendonk, 2010), indentified by HT gneissic gabric. Wang (1998) provided U-Pb zircon age of 2617+\-24 Ma, interpreted as minimum intrusive age. U-Pb zircon anaylsis of GSWA155513 yielded zircon ages of 2693+\-9 Ma, which may be intepreted as either a magmatic age or inherited component, and a younger concordant age of 2624 Ma, which may also represent a magmatic crystallisation age. Sample GSWA 207630 (porphyritic monzogranite) yielded a weighted mean 207Pb/206Pb date of 2626+\-6 Ma, interpreted as the magmatic crystallization age of the monzogranite. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv.|2637-2602 Ma|Unit of Bald Rock Supersuite.|Includes Cootharra Monzogranite, Garden Rock Monzogranite, Telegootherra Monzogranite, Walgoo Monzogranite, Wangata Monzogranite, Yarrabubba Monzogranite.|Crosscut by Marlomumbah Granite.|Monzogranite: k-feldspar porphyritic to megacrystic, muscovite and biotite rich with abundant pegmatite veins; syenogranite, granite, hornblende syenite, muscovite-rich pegmatite|
74845|Walganna Suite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|2647-2600 Ma (inferred)|Unit of Bald Rock Supersuite.|||Monzogranite, locally rich in muscovite and biotite; predominantly with equigranular texture and locally K-feldspar porphyritic; includes deeply weathered rock|
74845|Walganna Suite|71271|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton.|2650-2600 Ma.|Bald Rock Supersuite.|||Monzogranite, locally rich in biotite and muscovite; predominantly with equigranular texture and locally K-feldspar porphyritic; includes deeply weathered rock.|
74845|Walganna Suite|71272|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton.|2650-2600 Ma.|Bald Rock Supersuite.|||Monzogranite to syenogranite, undeformed, common magmatic foliation; (separately mapped) equigranular, medium- to coarse-grained monzogranite.|
74845|Walganna Suite|71809|5|Briefly described|map legend|Archean|Archean|Yilgarn Craton|~2650-2600 Ma|Of Bald Rock Supersuite.|Includes Seeligson Monzogranite.|||
74845|Walganna Suite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|||Walganna Suite|Includes Garden Rock Monzogranite, Telegoothera Monzogranite, and 3 unnamed units.||Porphyritic/megacrystic monzogranite; locally w biotite to 10%. Mainly equigranular monzogranite, locally rich in muscovite, biotite;  + locally porphyritic; includes deeply weathered rock. Monzogranite/syenogranite; undeformed; foliation common.|
74845|Walganna Suite|72389|5|Briefly described|Map Legend|Archean|Archean|Yilgarn Craton. Gabanintha 1:100k map sheet 2644.||Bald Rock Supersuite|||Monzogranite, locally rich in muscovite and biotite; predominantly with equigranular texture and locally K-feldspar phyric; includes deeply weathered rock.|28-AUG-20
78361|Walgoo Monzogranite|70140|5|Briefly described|Map legend.|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. 3 facies are mapped separately.||Walganna Suite.|||Monzogranite, locally rich in muscovite and biotite; predominantly with equigranular texture and locally K-feldspar porphyritic.|
78361|Walgoo Monzogranite|70770|5|Briefly described|Map legend.|Archean|Archean|Yilgarn Craton.|2647-2600 Ma.|Walganna Suite.|||Muscovite-bearing monzogranite, medium- to coarse-grained.|
78361|Walgoo Monzogranite|70796|5|Briefly described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton. See also 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, Bungar100_2539_stratig.pdf, Youanmi100_2640_stratig.pdf.|ca 2647 to 2600 Ma (inferred)|Walganna Suite|||Monzogranite, locally rich in muscovite and biotite; predominantly with equigranular texture and locally Kfeldspar porphyritic.  Muscovitebearing monzogranite; medium to coarse grained; marginal facies is pegmatitic and locally fluoritebearing.|
78361|Walgoo Monzogranite|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.|2650-2600 Ma (inferred)|Unit of Walganna Suite.|||Biotite and buscovite-bearing monzogranite; medium to coarse grained, locally k-feldspar porphyritic; marginal facies is pegmatitic and locally fluorite-bearing|
39503|Walgunya Trondhjemite|63417|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite. Geological Province: Pilbara Craton. Quartz-rich biotite trondhjemite; medium- to coarse-grained; metamorphosed.||||||07-NOV-08
39503|Walgunya Trondhjemite|63441|5|Briefly described|p8 Tb. 2|Archean|Archean|Of Emu Pool Supersuite. Geological Province: Pilbara Craton.||||||07-FEB-11
39503|Walgunya Trondhjemite|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of Emu Pool Supersuite.|||Quartz-rich biotite trondhjemite, medium- to coarse-grained, metamorphosed.|
39503|Walgunya Trondhjemite|65827|2|Defined|p6 Tb.2, p9 Fig 3, p25, p57|Paleoarchean|Paleoarchean|New name, after Walgunya Creek. Informally named Miningarra Trondhjemite (Sims and Carson 2001); previously of Chimingadgi Suite (Collins 1983).  Undated but probably 3324-3294 Ma. Resembles nearby Chimingadgi Trondhjemite. Mis-spelt as Trondjhemite (Fig.3) and as Walgunyah (Tb.2).||Of Emu Pool Supersuite.||Intrudes Apex Basalt.|Foliated, grey, med- to coarse-grained, quartz-rich biotite trondhjemite.|21-MAY-14
39503|Walgunya Trondhjemite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Emu Pool Supersuite|||Quartz-rich biotite trondhjemite; medium to coarse grained; weakly metamorphosed|
39503|Walgunya Trondhjemite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3325-3277 Ma (inferred)|Unit of Emu Pool Supersuite.|||Quartz-rich biotite trondhjemite; medium to coarse grained; weakly metamorphosed|
39503|Walgunya Trondhjemite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|||Emu Pool Supersuite|||Quartz-rich biotite trondhjemite; medium to coarse grained; weakly metamorphosed.|
38643|Wallaby Conglomerate|23786|5|Briefly described|p5|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
38643|Wallaby Conglomerate|24196|6|Mentioned|p47 Fig.5|||Geological Province: Laverton Domain, Yilgarn Craton.||||||
38643|Wallaby Conglomerate|62106|5|Briefly described|p1365|Archean|Archean|Age: <2675+/-4 Ma (SHRIMP U-Pb). Geological Province: Laverton greenstone belt in Eastern Goldfields province of Yilgarn Craton.||||||07-NOV-08
38643|Wallaby Conglomerate|63778|5|Briefly described|p1124|||Thickness: 1200m. Geological Province: Yilgarn Craton. Submarine fan-type deposit.||||||
38643|Wallaby Conglomerate|66880|6|Mentioned|pp18-19. |Archean|Archean|Stratigraphically correlated with Lancefield Conglomerate.|2673 +/- 5 Ma.|||||
38643|Wallaby Conglomerate|66937|5|Briefly described|p166, pp174-177.|Archean|Archean|At least 1500 m thick. Intruded by numerous dykes of monzonite, syenite and carbonatite. Aggradational to progradational style implies high subsidence rate and sediment flux, and sedimentation in a fixed-position canyon.||Unit in Wallaby Supersequence.||Overlies Brock Supersequence. Unconformably overlies Laverton Sequence. Is overlain by Potoroo Sandstone.|A clast-rich cobble conglomerate with rounded to well-rounded, compact to elongate clasts, mostly basalt and porphyritic dacite-rhyolite; matrix is coarse-grained quartzosericitic sandstone; metamorphic biotite common.|
38643|Wallaby Conglomerate|67198|5|Briefly described|p49, p55|||Hosts the Wallaby gold deposit. Occasionally referred to as the Wallaby conglomerate (p49-51). Detrital zircon age. A carbonatite intrusion is dated at 2664 +/- 3 Ma (Salier et al., 2004).|2663 +/- 5 Ma (Kositcin et al., 2008 U/Pb)||||Polymictic, clast-supported cobble conglomerate that is overlain by sandy turbidites and carbonaceous shale.|11-SEP-17
38643|Wallaby Conglomerate|72049|6|Mentioned|p257|||Geochronology analyses, results, and interpretation are discussed in detail.||||||
38643|Wallaby Conglomerate|73238|5|Briefly described|p5, 16-17, 26|||Laverton district, Eastern Goldfields Terrane.|c.2673 - 2664 Ma.|||||
38643|Wallaby Conglomerate|73391|6|Mentioned|p334|||A clastic sedimentary unit that wraps around the granite-cored dome at Mount Margaret.||||||
27250|Wallal Sandstone|7433|4|Described|p25 Fig.2, pp42-43, p52.|Oxfordian|Toarcian|Canning Basin. Continental to marine clastics. Contains a confined aquifer system.|||Includes Jurgurra Sandstone Member and Mudjalla Sandstone Member.|Underlies Alexander Formation and Callawa Formation.|In the north of the Basin, is exposed as sandstone, mudstone and conglomerate. In southwestern areas, drillholes indicate fluvial, deltaic and shallow marine components.|
27250|Wallal Sandstone|22717|5|Briefly described|P11, P12|Cretaceous|Jurassic|||||||
27250|Wallal Sandstone|22718|5|Briefly described|p5, Table1 p6|Cretaceous|Jurassic|||||||10-FEB-20
27250|Wallal Sandstone|22738|4|Described|10,13,16,17, map|Late Jurassic|Early Jurassic|Max thickness 500 m. Overlain by Alexander Formation, underlain by Noonkanbah Formation, Poole Sandstone, Grant Group.||||||26-JUL-07
27250|Wallal Sandstone|22741|5|Briefly described|p29, Table3 p11||Late Jurassic|||||||10-FEB-20
27250|Wallal Sandstone|22753|5|Briefly described|Fig.3 p585|Jurassic|Jurassic|||||||
27250|Wallal Sandstone|22765|5|Briefly described|p10, Table1|Late Jurassic|Middle Jurassic|Overlying unit is Alexander Foramtion, underlying unit is Noonkanbah Formation||||||10-FEB-20
27250|Wallal Sandstone|22767|5|Briefly described|Table3 p12, p23|Late Jurassic|Early Jurassic|||||||10-FEB-20
27250|Wallal Sandstone|22776|3|Fully described|p20, Table.3|Late Jurassic|Early Jurassic|? of Max age.||||||
27250|Wallal Sandstone|22801|5|Briefly described|p12, Table1 p8|Oxfordian|Toarcian|||||||10-FEB-20
27250|Wallal Sandstone|22814|5|Briefly described|fig2|Jurassic|Jurassic|||||||
27250|Wallal Sandstone|23212|4|Described|Table.1 p7|Late Jurassic|Middle Jurassic|||||||
27250|Wallal Sandstone|23415|5|Briefly described|Map Legend|Cretaceous|Jurassic|Geological province:  Westralian Superbasin. Sandstone with minor siltstone and conglomerate.||||||07-JAN-08
27250|Wallal Sandstone|23575|5|Briefly described|Map Legend|Mesozoic|Mesozoic|||||||
27250|Wallal Sandstone|23722|6|Mentioned|p35|Triassic|Triassic|||||||
27250|Wallal Sandstone|23757|4|Described|p16|Jurassic|Jurassic|Unconformably overlies Muccan Granitoid Complex. Thickness northwards: >200m. Geological Province: Westralian Superbasin. Consists of fine- to very coarse-grained sandstone with interbedded conglomerate units increasing towards base.||||||13-DEC-22
27250|Wallal Sandstone|23765|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||
27250|Wallal Sandstone|23766|4|Described|p13 Tb. 2|Late Jurassic|Early Jurassic|Consists of laminated pink and white, very fine to very coarse-grained sandstone with minor siltstone, conglomerate and lignite. Thickness: 286m. See also p26.||||||26-AUG-08
27250|Wallal Sandstone|24061|5|Briefly described|p182|Jurassic|Jurassic|Geological Province:  Canning Basin.||||||
27250|Wallal Sandstone|24062|5|Briefly described|p186 Table 1|Jurassic|Jurassic|Geological Province: Canning Basin.||||||
27250|Wallal Sandstone|24449|5|Briefly described|p744|Oxfordian|Callovian|Age: ~150m.y.  Geological Province: Canning Basin.  See also p741 Fig. 2.||||||
27250|Wallal Sandstone|30110|6|Mentioned|p81|||See also p84.Middle - Upper Jurassic, Bajocian - Callovian age.||||||10-FEB-20
27250|Wallal Sandstone|30313|5|Briefly described|p54|||Jurassic age||||||
27250|Wallal Sandstone|30897|6|Mentioned|p19|||Subsurface unit||||||
27250|Wallal Sandstone|32648|6|Mentioned|p32|||U.Jur.||||||
27250|Wallal Sandstone|33166|6|Mentioned|p67|||Stratigraphy||||||
27250|Wallal Sandstone|34134|6|Mentioned|Cor.Chart|||Middle - Upper Jurassic.||||||
27250|Wallal Sandstone|34363|6|Mentioned|p56|||Middle Jurassic. See also Fig.7.||||||
27250|Wallal Sandstone|35275|6|Mentioned|Fig.5.|||||||||
27250|Wallal Sandstone|35711|4|Described|p25|||See also Table 3,stratigraphy. Hydrogeology on p51.||||||26-JUL-07
27250|Wallal Sandstone|35969|6|Mentioned|p66|||Hydrogeology discussed P70.||||||
27250|Wallal Sandstone|36224|5|Briefly described|Map legend|Early Jurassic|Early Jurassic|Sandstone, minor siltstone, conglomerate, lignite.  Early? to Late Jurassic.||||||01-FEB-05
27250|Wallal Sandstone|36225|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
27250|Wallal Sandstone|36268|5|Briefly described|p175|Jurassic|Jurassic|Geological Province: Canning Basin.  Yields ground water with low salinity.||||||07-JAN-15
27250|Wallal Sandstone|36438|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|Early? to Late Jurassic.||||||
27250|Wallal Sandstone|36634|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|Early ? to Late Jurassic.||||||
27250|Wallal Sandstone|36890|3|Fully described|p344|||||||||
27250|Wallal Sandstone|37364|6|Mentioned|p1050|||||||||
27250|Wallal Sandstone|37368|6|Mentioned|Map legend|Late Jurassic|Early Jurassic|Early to Late Jurassic||||||
27250|Wallal Sandstone|37369|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|Early? to Late Jurassic||||||
27250|Wallal Sandstone|37370|6|Mentioned|Map legend|Late Jurassic|Early Jurassic|Early to Late Jurassic||||||
27250|Wallal Sandstone|37564|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|Early? to Late Jurassic||||||
27250|Wallal Sandstone|38878|6|Mentioned|Map legend|Late Jurassic|Early Jurassic|Early - Late Jurassic||||||
27250|Wallal Sandstone|38886|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|Early ? to Late Jurassic||||||
27250|Wallal Sandstone|39857|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|Early? to Late Jurassic||||||
27250|Wallal Sandstone|40045|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|Early ? to Late Jurassic||||||
27250|Wallal Sandstone|40078|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|Early? to Late Jurassic||||||
27250|Wallal Sandstone|40992|6|Mentioned|Fig.11|||||||||
27250|Wallal Sandstone|41169|6|Mentioned|Fig.3|||||||||
27250|Wallal Sandstone|41436|6|Mentioned|p46|||||||||
27250|Wallal Sandstone|41688|4|Described|p15|||See also p19.||||||26-JUL-07
27250|Wallal Sandstone|42338|5|Briefly described|Table 1 p145|||||||||10-FEB-20
27250|Wallal Sandstone|42571|4|Described|p18, Table1 p9|||||||||
27250|Wallal Sandstone|42572|5|Briefly described|Map Legend|Jurassic||||||||23-DEC-09
27250|Wallal Sandstone|42734|5|Briefly described|map legend|Jurassic||||||||
27250|Wallal Sandstone|42792|5|Briefly described|Table 1 p225|||||||||10-FEB-20
27250|Wallal Sandstone|42814|5|Briefly described|p24|||||||||
27250|Wallal Sandstone|42930|5|Briefly described|Fig.1 p473|Late Jurassic|Late Jurassic|Unconformably overlain by Alexander Formation; interfingers with a lateral equivalent unit, Barbwire Sandstone. Geological Province: Canning Basin. Marine. deltaic deposits.||||||13-NOV-07
27250|Wallal Sandstone|43173|6|Mentioned|12|Middle Jurassic|Early Jurassic|||||||
27250|Wallal Sandstone|43563|6|Mentioned|Fig.2,p5|Late Jurassic|Middle Jurassic|||||||
27250|Wallal Sandstone|43656|6|Mentioned|Fig.2,p8|Oxfordian|Aalenian|||||||
27250|Wallal Sandstone|43666|6|Mentioned|p45,Table 2|Oxfordian|Bajocian|||||||
27250|Wallal Sandstone|43746|6|Mentioned|Fig.2,p11|Oxfordian|Aalenian|||||||
27250|Wallal Sandstone|43818|6|Mentioned|Fig.2.p39|Late Jurassic|Early Jurassic|||||||
27250|Wallal Sandstone|44143|4|Described|p433 Table 4-19; p448-449|Jurassic|Jurassic|Up to 400m thick; sandstone; minor siltstone, conglomerate and lignite; continental to shallow marine. Type section between 276 and 584m in Wallal 4 (MANDORA: 19deg 44' 12"S, 120deg 44' 25" E). Contains abundant microfauna and microflora; Toarcian to Oxfordian.||||||
27250|Wallal Sandstone|44357|4|Described|p12,Tb.1 p9||Jurassic|Subsurface only.||||||
27250|Wallal Sandstone|44443|5|Briefly described|map legend|Late Jurassic|Late Jurassic|||||||
27250|Wallal Sandstone|45153|2|Defined|App.6-94|Late Jurassic|Early Jurassic|Early to Late Jurassic.||||||24-NOV-08
27250|Wallal Sandstone|45156|6|Mentioned|p31|||Correlative||||||
27250|Wallal Sandstone|45158|3|Fully described|p16|||||||||
27250|Wallal Sandstone|45168|6|Mentioned|p6|||||||||
27250|Wallal Sandstone|46319|4|Described|p17|Late Jurassic|Middle Jurassic|Geological Province: Canning Basin.||||||
27250|Wallal Sandstone|46860|6|Mentioned|p314|||||||||
27250|Wallal Sandstone|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
27250|Wallal Sandstone|48596|14|Not recorded|p.5|||(E51-11)||||||
27250|Wallal Sandstone|50544|5|Briefly described|p16 Tb. 1|Jurassic|Jurassic|Overlies the Grant Group on central northern margin of YARRIE (not shown on sheet).  Age: 189.6-154.1Ma.  Geological Province: Canning Basin.  See also p62.||||||
27250|Wallal Sandstone|50555|5|Briefly described|Map legend|Cretaceous|Jurassic|Fine to coarse-grained sandstone and conglomerate. Geological Province: Canning and Northern Carnarvon Basins (Westralian Superbasin).||||||26-AUG-08
27250|Wallal Sandstone|61021|5|Briefly described|p36 Fig. 2|Oxfordian|Bajocian|Geological Province: Canning Basin.||||||17-DEC-07
27250|Wallal Sandstone|63420|5|Briefly described|Map legend|Cretaceous|Jurassic|Sandstone, minor siltstone and conglomerate (sub-surface only).||||||
27250|Wallal Sandstone|64185|5|Briefly described|p158 Fig. 2, p165|Early Cretaceous|Middle Jurassic|Underlain unconformably by Grant Formation. Marine. See p165 for more information.||||||
27250|Wallal Sandstone|64186|5|Briefly described|p171, p170 Fig. 1|Callovian|Callovian|Overlain by Alexander Formation underlain by Poole Sandstone. Max thickness: 308m.||||||
27250|Wallal Sandstone|64580|4|Described|map legend||Early Jurassic|Sandstone; minor siltstone and conglomerate.||||||24-NOV-08
27250|Wallal Sandstone|64643|5|Briefly described|p3 Fig. 2|Upper Jurassic|Middle Jurassic|||||||
27250|Wallal Sandstone|64982|6|Mentioned|p700.|||||||||
27250|Wallal Sandstone|65301|5|Briefly described|p5 Fig. 4|Late Jurassic|Middle Jurassic|Geological province: Canning Basin.||||||
27250|Wallal Sandstone|65449|5|Briefly described|p6, p47-48|Late Jurassic|Middle Jurassic|Overlies Carribuddy Group and/or Worral Formation in Frome Rocks 1. Appears only as Wallal.||||Is overlain by Alexander Formation. Lateral equivalent of Barbwire Sandstone.||
27250|Wallal Sandstone|67202|6|Mentioned|p43, p44 Fig.2.10|Jurassic|Jurassic|One of the dominant aquifers in the Canning Basin.||||Unconformably overlies the Noonkanbah Formation.||15-FEB-18
27250|Wallal Sandstone|68007|6|Mentioned|p4, p8|Late Jurassic|Middle Jurassic|Canning Basin. Interpreted as 32.5m thick (245.5 - 278 m) in Patience 1 well, Menzel and Lipski (1986). No biostratigraphic data presented.||||||19-FEB-20
27250|Wallal Sandstone|68283|5|Briefly described|Map Legend||Jurassic|Canning Basin.|||||Sandstone; minor siltstone and conglomerate (subsurface only).|07-JAN-15
27250|Wallal Sandstone|68811|5|Briefly described|p79, p80, p81|Jurassic|Jurassic|Seawater intrusion has been measured within this units aquifer. See also p127 tbl 14, p154 app 1, p174 tbl 35. ||||Underlies the Jarlemai Siltstone. Overlies the Erskine Sandstone and the Munkyarra Shale.||15-APR-20
27250|Wallal Sandstone|68902|6|Mentioned|p9 fig 5|Jurassic|Jurassic|||||Overlain by Alexander Formation.||
27250|Wallal Sandstone|69029|6|Mentioned|p319|Oxfordian|Bajocian|Of Canning Basin.||||Overlain by Alexander Formation. Underlain by Blina Shale.||
27250|Wallal Sandstone|69182|6|Mentioned|Ch4 p3, Ch4 p9, Ch4 p30-p35|Middle Jurassic|Middle Jurassic|Canning Basin. See also Ch4 p45, Ch4 p64-p65, Ch4 p83-p84, Ch4 p87. ||||Overlain by the Alexander Formation.||
27250|Wallal Sandstone|69312|5|Briefly described|p3|Oxfordian|Bajocian|Canning Basin. ||||Faulted against the Blina Shale [?]. Overlain by the Alexander Formation.|Sandstone.|11-FEB-20
27250|Wallal Sandstone|70154|5|Briefly described|500k_interpgeop14_lut.csv|Oxfordian|Middle Jurassic||157-174 Ma||||Sandstone; minor siltstone and conglomerate|
27250|Wallal Sandstone|70774|5|Briefly described|p4, p32|Late Jurassic|Middle Jurassic|Fitzroy Trough, Lennard Shelf and Willara and Kidson Sub-basins, Canning Basin.||||Overlain by the Alexander Formation. Equivalent to the Barbwire Sandstone.||10-FEB-20
27250|Wallal Sandstone|70826|6|Mentioned|p7 tbl 4|Early Cretaceous|Jurassic|Canning Basin.||||||
27250|Wallal Sandstone|71267|5|Briefly described|1m_geologyp12_lithology_lut.csv|Oxfordian|Middle Jurassic|Of Canning Basin. See 1m_geologyp12_lithology_lut.csv, 500k_interpgeop16_lut.csv.|174.1-157.3 Ma (biostrat)||||sandstone, siltstone, conglomerate, lignite|
27250|Wallal Sandstone|71894|5|Briefly described|p3|Jurassic|Jurassic|Canning Basin. Relatively uniform in thickness from north to south but thins from the west to the east.||||Unconformably overlies the Blina Shale. Overlain by the Alexander Formation.|Sandstone.|
27250|Wallal Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Oxfordian|Middle Jurassic|Canning Basin.  Age from biostratigraphy.|||||Sandstone; minor siltstone and conglomerate.|
27250|Wallal Sandstone|72497|5|Briefly described|p3 Fig.2.|Callovian|Aalenian|Shown as occuring in the Anketell, Tabletop, Ryan Shelves, Willara and Kidson Sub-basins, the Jurgurra and Barbwire Terraces and Broome Platform. Also shown as occuring in the Fitzroy Trough, Betty and Balgo Terraces and part of the Lennard Shelf and Margaret Terrace. Diachronous base. Older in south. Age range shown as Aalenian-Callovian.||||Conformably underlies Alexander Formation and partly laterally equivalent to Barbwire and Meda Sandstones. Unconformably overlies Blina Shale, Erskine & Culvida Sandstones.||
27250|Wallal Sandstone|72499|4|Described|p7 Fig.6, p10, p70, p86|Late Jurassic|Middle Jurassic|Located in the Willara Sub-basin and the Broome Platform. Thickness range of 89-174m reported in study area. Sandstone formed in fluvio-deltaic settings. Considered to host an important shallow groundwater aquifer in the western Canning Basin. Ref Forman and Wales, 1981.||||Shown as unconformably overlying Blina Shale, Liveringa Formation. Underlies Alexander Formation. Partial lateral equivalent to Barbwire Sandstone.|Dominantly sandstone.|
27250|Wallal Sandstone|73117|5|Briefly described|p3|Middle Jurassic|Middle Jurassic|Canning Basin. Lower boundary marked by a major unconformity [related to the Fitzroy Transpression?].||||Overlain by Alexander Formation. Equivalent to Barbwire Sandstone.|Dominantly sandstone.|
78876|Wallara Formation|70416|5|Briefly described|p64, p65 Fig.2|Cryogenian|Cryogenian|Amadeus Basin. Previously the informal Finke beds. Now includes part of the former Boord Formation.||||Correlated with lower part of Inindia beds.||
78876|Wallara Formation|70839|5|Briefly described|p329|Neoproterozoic|Neoproterozoic|Of Amadeus Basin.||||Overlain by Areyonga Formation. Underlain by Bitter Springs Formation or Pinyanna beds.||
78876|Wallara Formation|71001|6|Mentioned|p21, 23-24|Tonian|Tonian|Amadeus Basin. Formerly known as the Finke Beds.||||Overlies Johnnys Creek Formation.|Black pyritic shales interbedded with dolostone and minor red siltstone.|
78876|Wallara Formation|71080|5|Briefly described|p27, p29 fig 20, p30, 31|Tonian|Tonian|Amadeus Basin. Upper supersequence 1. Recently recognised (Normington et al. 2015). Previously refered to as 'Finke beds', 'Johnnys Creek beds'. Probable paleo-oil column identified in this unit based on grain fluorescence studies (Marshall et al., 2007).|||||Dominantly carbonate-shale, marl.|
78876|Wallara Formation|71088|6|Mentioned|p8|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
78876|Wallara Formation|71279|6|Mentioned|p355 Fig.2|Cryogenian|Cryogenian|Amadeus Basin.||||||
78876|Wallara Formation|71344|5|Briefly described|p1094, 1093, 1095, 1096, 1102-3|Tonian|Tonian|Amadeus Basin. Limited exposure and occurrence.|~750 Ma||||Interbedded dolostone, dolomitic siltstone and shale with occasional pyrite and glauconite.|10-NOV-17
78876|Wallara Formation|71810|5|Briefly described|Map legend.|Tonian|Tonian|Amadeus Basin (Phase 1), Centralian Superbasin.|||||Dolomite, oolitic dolomite, sandstone and siltstone; stromatolitic, commonly silicified to chert and sandy chert at surface.|
78876|Wallara Formation|71841|5|Briefly described|iii,p1-2,9-11,13-14|Cryogenian|Cryogenian|Of Amadeus Basin. Previously informally termed finke beds. Renamed Wallara Formation; formalised by Normington et al (2015), Normington and Donnellan (in review). Revised stratigraphy in drill core: indentified in CPD003 at 181.3-201.1m. See p9-11 (CPD003) for lithological descriptions based on revised drill core intervals.||||||
78876|Wallara Formation|71842|4|Described|iii,p2-5,9|Cryogenian|Cryogenian|Of Amadeus Basin. Part of revised nomenclature after this study in the Mount Conner area. Formerly known as Finke Beds (this name is now superseded; Normington et al 2015; Normington and Donnellan in review). Originally identified in wells in the central part of the basin, has since been recognised in outcrop in the far west of the basin in WA (Haines et al., 2010) and central north/central part of the basin (HENBURY; Donnellan and Normington 2017). Contains diagnostic stromatolite Bacalia burra; recorded in most exposures (Allen et al 2012, Haines and Allen 2014, Normington et al 2015) and in drillholes (Grey et al 2012).||||Overlain by Areyonga Formation. Underlain unconformably by Bitter Springs Group. Probably overlies the Loves Creek Formation. Equivalent to/replaces Finke Beds.|Sandstone, siltstone, chert (surface exposures only) and carbonate lithofacies.|08-JAN-20
78876|Wallara Formation|72375|4|Described|p1-2,13,15-17|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Formerly known as Finke beds, newly formalised term of Normington et al., 2015. Type section in drillhole: Wallara-1. Recognised in several stratigraphic and petroleum exploration wells in the central and centralnorthern part of the Amadeus Basin (eg drillholes Wallara 1 and Finke 1; Edgoose 2013). Expressed in outcrop as a silicified regolith unit or paleosurface overlying Johnnys Creek Formation. Inferred to be Cryogenian (c. 720-635 Ma) based on first occurrence of the acritarch Cerebrosphaera buickii (Grey et al., 2011). LA-ICP-MS U-Pb isotopic analysis by Normington et al., 2016 yielded an interpreted max depositional age (youngest individual zircon) of 1006+\-13 Ma. LA-ICP-MS Hf isotopic signatures for the zircon age populations of sample NTGS HB14VJN001 (very coarse- to coarse-grained sandstone) suggest they crystallised in magmas derived from a range of crustal sources (see p16 for Hf isotopic results and interpretations).||||Overlain by Areyonga Formation. Underlain disconformably by Johnnys Creek Formation.|In drill core: stromatolitic and micritic dolostone, and fine- to coarse grained sandstone with siltstone and dolomitic siltstone intervals.|
78876|Wallara Formation|72601|5|Briefly described|p3, p7, p9-12, p14, p17, p25|Tonian|Tonian|Amadeus Basin. Shallow marine setting. Contains the biostratigraphic marker stromatolite Baicalia burra (Grey et al., 2012). Previously [included?] the informal Finke beds (name invalid). Palynomorph assemblages have less diversity than underlying units, but contain the distinctive species Cerebrosphaera buickii.||||Unconformably underlain by Johnnys Creek Formation (Bitter Springs Group). Unconformably overlain by Areyonga Formation.|Ooid chert and carbonates.|
78876|Wallara Formation|73085|4|Described|piii, p1-3, p5, p15-16, p20, p22, p24-27|Tonian|Tonian|Amadeus Basin. Previously 'Finke beds'. Contains diagnostic stromatolite taxa. Includes the acritarch Cerebrosphaera buickii, which is an important global time marker for the late Tonian both nationally and internationally. 104.7 m thick in drillhole BR05DD01. Capped by a ~2m buff, silicified sedimentary breccia that has a sharp contact with the overlying Areyonga Formation. Basal contact with Johnnys Creek Formation is transitional.||||Unconformably[?] underlain by Johnnys Creek Formation (Bitter Springs Group). Unconformably[?] overlain by Areyonga Formation and Inindia beds.|Alternating silicified, buff carbonate rocks and red and silicified, buff to grey siltstone with calcite-filled voids and veins; carbonate intervals are variably stromatolitic.|
78876|Wallara Formation|73086|1|Redefined|[See comments].|Cryogenian|Cryogenian|[Redefined herein. See also definition card, ASUD]. New name; previously known as Finke beds. Amadeus Basin. Part of Supersequence I. Typically exposed as silcrete and ferricrete. Contains the first appearance of the acritarch Cerebrosphaera buickii in the Amadeus Basin. A detrital zircon maximum depositional age of 1023 +/- 34 Ma (U-Pb LA-ICP-MS) is significantly older than the suspected true depositional age. Areyonga Movement resulted in uplift and erosion of parts of the Heavitree - Wallara Formation succession. Upper contact is marked by a 90 cm-thick interval of brecciated dolostone interpreted to be palaeokarst. Unconformably underlain by Heavitree Formation in places. p: iii, 3, 5-7, 39, 53, 56-60, 62, 143, 156, 158, App 2.||||Underlain by Johnnys Creek Formation (Bitter Springs Group). Unconformably overlain by Areyonga Formation. Correlates to Inindia beds, Buldya Group, Burra Group, Browne Formation, Hussar Formation.|Predominantly dolostone, quartz sandstone, feldspathic quartz sandstone, and red and green mudstone; with subordinate dark carbonaceous mudstone and shale and arkosic sandstone.|
78876|Wallara Formation|73088|6|Mentioned|p1|Tonian|Tonian|Amadeus Basin, northeast. Previously called Finke beds.||||Underlain by Johnnys Creek Formation (Bitter Springs Group). Unconformably overlain by Areyonga Formation.||
78876|Wallara Formation|73180|5|Briefly described|p48 Fig.1, p49|Neoproterozoic|Neoproterozoic|Amadeus Basin. Locally separates the underlying Bitter Springs Group from the overlying Areyonga Formation, suggested to be bounded by disconformities.||||Disconformably overlies the Bitter Springs Group, disconformably underlies the Areyonga Formation.|Mixed sandstone, siltstone and dolostone sequence.|
78876|Wallara Formation|73346|6|Mentioned|p28|Tonian|Tonian|Amadeus Basin.||||||
35243|Wallareenya Granodiorite|23789|6|Mentioned|p30 Fig. 11|||||||||
35243|Wallareenya Granodiorite|24166|4|Described|p14|Archean|Archean|Of the Pippingarra Granitoid Complex||||||07-NOV-08
35243|Wallareenya Granodiorite|24327|5|Briefly described|Map Legend|Archean|Archean|Of the Pippingarra Granitoid Complex. Hornblende-biotite granodiorite and tonalite.  Age: 2955Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
35243|Wallareenya Granodiorite|24349|5|Briefly described|Map legend|Archean|Archean|Of the Pippingarra Granitoid Complex.  Age: <3475Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
35243|Wallareenya Granodiorite|63420|5|Briefly described|Map legend|Archean|Archean|Of the Sisters Supersuite. Age: c.2955Ma. Geological Province: Pilbara Craton. Hornblende-biotite granodiorite and tonalite; massive to moderately foliated; locally inclusion-rich; metamorphosed.||||||07-NOV-08
35243|Wallareenya Granodiorite|63441|5|Briefly described|p11 Tb. 2, p37|Archean|Archean|Of Indee Suite (Sisters Supersuite). Age: 2954+/-4Ma. Geological province: Pilbara Craton.  Intrudes De Grey Supergroup.||||||07-FEB-11
35243|Wallareenya Granodiorite|67201|6|Mentioned|p22 Fig.13|||In De Grey Superbasin.||||||
35243|Wallareenya Granodiorite|68283|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|c.2955 Ma|Of the Sisters Supersuite.|||Hornblende-biotite granodiorite and tonalite; massive to moderately foliated; locally inclusion rich; metamorphosed.|
35243|Wallareenya Granodiorite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Sisters Supersuite|||Hornblende--biotite granodiorite and tonalite; massive to moderately foliated; locally inclusion-rich; weakly metamorphosed|
35243|Wallareenya Granodiorite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; North Pilbara Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|2954 Ma (isotopic)|Unit of Sisters Supersuite.|||Hornblende-biotite granodiorite and tonalite; massive to moderately foliated; locally inclusion-rich; weakly metamorphosed|
35243|Wallareenya Granodiorite|70775|6|Mentioned|p65|||||Indee Suite||||
35243|Wallareenya Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite, tonalite|
35243|Wallareenya Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||2954+/-4 Ma.|Indee Suite|||Hornblende--biotite granodiorite and tonalite; massive to moderately foliated; locally inclusion-rich; weakly metamorphosed.|
68516|Waloo Waloo Monzogranite|63441|2|Defined|p10 Tb. 2, p37|Archean|Archean|Of the Maitland River Supersuite. Unconformably overlain by Hardey Formation. Age: 2988+/-7Ma. Geological province: Pilbara Craton. Forms the south-eastern portion of the Cherratta Granitic Complex.||||||07-FEB-11
68516|Waloo Waloo Monzogranite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Maitland River Supersuite. Geological province: Pilbara Craton.  Biotite monzogranite; medium-grained; weakly foliated; metamorphosed.||||||07-NOV-08
68516|Waloo Waloo Monzogranite|64580|4|Described|map legend||Mesoarchean|Of Maitland River Supersuite. Biotite monzogranite, medium grained; weakly foliated; metamorphosed.||||||15-DEC-08
68516|Waloo Waloo Monzogranite|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Maitland River Supersuite.|||Biotite monzogranite, medium grained; weakly foliated; metamorphosed|
68516|Waloo Waloo Monzogranite|70775|5|Briefly described|p53|Mesoarchean|Mesoarchean|Together with the Jean Well Granodiorite, Whyjabby Granodiorite, Brill Monzogranite, Toorare Tonalite and Mardeburra Granodiorite comprises the Cherratta Granitic Complex.|2988 +/- 7 Ma (SHRIMP, Nelson, 2001j)|Maitland River Supersuite|||Foliated biotite monzogranite.|
68516|Waloo Waloo Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
68516|Waloo Waloo Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|De Grey Superbasin.|2988+/-7 Ma.|Maitland River Supersuite|||Biotite monzogranite; medium grained; weakly foliated; metamorphosed.|
77241|Walpa suite|66256|5|Briefly described|p8, p18 Fig.14, p23-32, see comments|Ectasian|Ectasian|Age: early Musgravian. Walpa Pulka Zone. Systematic compositional variation that parallels northwest trend of major shear zones. Geochemistry provided. SHRIMP whole rock Nd isotopic crystallisation age. Metamorphic age: Walpa Pulka Zone 1171+/-12 to 1174 +/-11 Ma. See also p35-38, p41, p43-44, p53 App.1, p67-68 App.3.|1219+/-12 Ma to 1215+/-13 Ma (GSWA).|Pitjantjatjara Supersuite||||11-JAN-17
77241|Walpa suite|67375|6|Mentioned|p25 Fig.17, p26 Fig.19. |Mesoproterozoic|Mesoproterozoic|A-type. Yb-enriched, within-plate granite. Early Musgrave Orogeny.||Unit in Pitjantjatjara Supersuite.||||
77241|Walpa suite|67553|6|Mentioned|p27-28,33|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province, North Australian Craton. Early Musgravian granite.||Unit of Pitjantjatjara Supersuite.||||
77241|Walpa suite|69091|6|Mentioned|p64 Fig.4.10|||early Musgravian granite|||||Granite.|
77241|Walpa suite|69729|5|Briefly described|p74 Fig.7, p77-78|||Geochemistry plots.||Pitjantjatjara Supersuite.|||A-type granites.|
24071|Walter Williams Formation|22534|4|Described|p13, Fig.4 p7|||Of Linger and Die Group.||||||24-JUN-09
24071|Walter Williams Formation|22596|6|Mentioned|Fig.9 p419|||||||||
24071|Walter Williams Formation|22640|6|Mentioned|p298|||||||||
24071|Walter Williams Formation|22676|6|Mentioned|Fig23,p301|||||||||
24071|Walter Williams Formation|22890|6|Mentioned|P17||Archean|Age of unit is 2710 Ma and 2692 Ma||||||07-NOV-08
24071|Walter Williams Formation|23132|4|Described|p335-336|||||||||
24071|Walter Williams Formation|23782|4|Described|p6|||Maximum thickness: ~180m.  Geological Province: Yilgarn Craton.||||||
24071|Walter Williams Formation|24139|5|Briefly described|p239 Table 1|||Geological Province: Ora Banda Domain.  Of the Linger and Die Group.||||||
24071|Walter Williams Formation|24229|5|Briefly described|p161, p162 Fig.2|Archean|Archean|Unit referred to as WWF throughout text.||||||07-NOV-08
24071|Walter Williams Formation|24494|6|Mentioned|p12|||||||||
24071|Walter Williams Formation|42221|6|Mentioned|p9|||||||||
24071|Walter Williams Formation|42382|4|Described|p16|||||||||
24071|Walter Williams Formation|42696|6|Mentioned|Plate 1B|||||||||
24071|Walter Williams Formation|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
24071|Walter Williams Formation|42870|5|Briefly described|Table 1, P67|||||||||
24071|Walter Williams Formation|42989|5|Briefly described|Fig.2,Fig.4|||||||||
24071|Walter Williams Formation|43074|6|Mentioned|Fig.4|||||||||
24071|Walter Williams Formation|43101|5|Briefly described|Table 1.|||of Linger and Die Group||||||
24071|Walter Williams Formation|43102|5|Briefly described|p8|||||||||
24071|Walter Williams Formation|43162|4|Described|5-24|||||||||
24071|Walter Williams Formation|43496|6|Mentioned|6|||||||||
24071|Walter Williams Formation|43574|6|Mentioned|Fig.1,p298|||||||||
24071|Walter Williams Formation|50075|5|Briefly described|p7|Archean|Archean|Of Hill et al (1995, 2001). Geological Province: Yilgarn Craton.||||||07-NOV-08
24071|Walter Williams Formation|60076|5|Briefly described|p12 Tb. 2, p18|||Olivine cumulates.  Max. thickness: <400m. Geological Province: Ora Banda domain (Yilgarn Craton).||||||
24071|Walter Williams Formation|60514|5|Briefly described|p65 Table 1.|Archean|Archean|Of the Linger and Die Group. Overlain by Siberia Komatiite. Geological Province: Ora Banda Domain.||||||07-FEB-11
24071|Walter Williams Formation|60627|5|Briefly described|p65 Tb.1|||Of Linger and Die Group.||||||
24071|Walter Williams Formation|63712|6|Mentioned|p838, p839 Fig. 7|||Sheet-like morphology at Kurrajong in Western Australia. See also p842.||||||
24071|Walter Williams Formation|63981|6|Mentioned|p93 Fig.3, |Archean|Archean|Ora Banda Domain. Kambalda Sequence. |||||Komatiite and high MgO basalt.|
24071|Walter Williams Formation|64771|4|Described|p9, p11-16|||Gole and Hill (1990), Hill et al. (1995). East Ida greenstone belt. Extends 35x130km; part of a very large flow field. It is layered; thickness up to 800m. CaO increases, MgO decreases upwards from base. Described in detail.|||||Olivine cumulates, serpentinised and silicified, and upper gabbro. A strongly cleaved grey shale/slate unit within the ultramafic unit was probably an interflow sediment.|
24071|Walter Williams Formation|65204|5|Briefly described|pg6 Tbl.1, p10, p24|Archean|Archean|Of Linger and Die Group. Komatiitic flows and/or massive olivine adcumulate; has preserved cumulate textures; underlies nickel-cobalt deposits.||||||
24071|Walter Williams Formation|65264|6|Mentioned|p16|||Of Hill et al (1990) and Witt (1994b). A komatiite unit in the Ora Banda area.||||||07-FEB-11
24071|Walter Williams Formation|65834|6|Mentioned|p7|||Ora Banda Domain, Kalgoorlie Terrane.||Linger and Die Group.||||
24071|Walter Williams Formation|68109|5|Briefly described|p660|Neoarchean|Neoarchean|Of Hill et al.(1995), for extensive ultramafic cumulates in the northern Kalgoorlie Terrane. Age constrained by U-Pb zircon ages of volcanic and sedimentary rocks associated with komatiites in the area. |ca. 2704 Ma - >2692 Ma.||||Ultramafic cumulates.|
24071|Walter Williams Formation|68289|5|Briefly described|p18-p20, p27-p28|||Traceable over an area of about 35 by 130km. Interpreted as part of a very large komatiite flow field.||||Overlain by the Siberia Komatiitic Volcanics.|Olivine cumulates and upper gabbroic rocks.|
24071|Walter Williams Formation|69152|6|Mentioned|geochron file 185901.1.pdf|||Mentioned as unit underlying material dated. See geochron file 185901.1.pdf (2010).|||||includes pyroxene-spinifex textured basalt at top|
24071|Walter Williams Formation|69631|5|Briefly described|p30, p33-34, p50-51|Siderian|Siderian|Gore and Hill (1990), Hill et al. (1995). A layered body, c.35 x 130 km, interpreted as part of a very large komatiitic flow field. From 50m up to 900m thick. Stratigraphic profiles.||||Is overlain by Siberia Komatiite.|Comprises a lower zone of olivine adcumulate, minor olivine orthocumulate, harrisite, and an upper zone of gabbroic rocks. Local strongly cleaved grey shale/slate (interflow sediment). Capped by dark brown siliceous laterite.|
24071|Walter Williams Formation|70153|5|Briefly described|185901.1.pdf|Archean|Archean|Conformably overlain by thinly bedded metasedimentary rock from which this sample was taken. Sample description: (185901.1.pdf). Maximum depositional/eruption age.|2695 +/- 5 Ma (U-Pb SHRIMP detrital zircon).||||Pyroxene spinifex textured basalt.|
24071|Walter Williams Formation|70276|6|Mentioned|p786|||Kalgoorlie terrane, Yilgarn Craton. Distal intrusive facies.|||||Sheet dunites.|
24071|Walter Williams Formation|70326|5|Briefly described|p360|Neoarchean|Neoarchean|Geological province: Ora Banda region, Ora Banda Domain, Kalgoorlie Terrane, Yilgarn Craton. ||||Overlain by Siberia Komatiite. Underlain by Missouri Basalt.||
24071|Walter Williams Formation|70773|5|Briefly described|iv, p1, p15, p46, p48-p50, p52, p58|||Norseman-Wiluna greenstone belt. North from Yunndaga the upper zone of this formation is a layered gabbro which thickens from 3-40m at Yunndaga to 180m at Kurrajong. Total thickness of this unit is unconstrained due to lack of dip information and sediment cover.||||Overlain by the Siberia Komatiite.|Dunites, cumulate and non-cumulate komatiitic gabbros.|
24071|Walter Williams Formation|71166|5|Briefly described|p19|||Effective hydraulic seal for gold mineralisation. ||||||
24071|Walter Williams Formation|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2726-2680 Ma (inferred)|Unit of Vetters Subgroup.|||Peridotite; relict olivine cumulate texture; commonly serpentinized or silicified|
24071|Walter Williams Formation|73391|5|Briefly described|p53, Appendices.|||Witt (1990). Ora Banda Domain, Kalgoorlie Terrane. Appears as Walter Williams dunite on p53.||||Overlies Missouri, Wongi Basalts. Is overlain by Siberia Komatiite.|Adcumulate dunite with upper and lower olivine orthocumulate margins, leucogabbro.|
42366|Walungurru Volcanics|61387|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Felsic to intermediate rocks (including silicified cryptocrystalline, porphyritic andesite and dacite); and, mafic to intermediate rocks (including silicified microcrystalline basalt, metad.  Of the Kintore Domain, Warumpi Province.  In the Arunta region.||||||07-NOV-08
42366|Walungurru Volcanics|61519|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Warumpi Province.||||||07-NOV-08
42366|Walungurru Volcanics|64580|4|Described|map legend|Devonian|Paleoproterozoic|Dacitic and rhyodacitic volcanic rocks.||||||04-DEC-15
42366|Walungurru Volcanics|64677|5|Briefly described|v, p1, p33-35, p52-63|||Arunta Region, Warumpi Province. Felsic extrusive rocks. Complex zircon age spectrum discussed. This is a conservative age: the youngest concordant analysis is 1617 +/- 14 Ma.|1699 +/- 14 Ma (maximum extrusion age).||||Dark, very fine-grained, quartz- and feldspar-phyric dacite; flow banding, flattened possible fiamme or shards.|
42366|Walungurru Volcanics|67565|6|Mentioned|p5 Fig.3.|||Warumpi Province.||||||
42366|Walungurru Volcanics|68994|4|Described|p1, p4, p6-11, p17, p23-27|||Kintore Domain in Warumpi Province. Its role in a speculative model of tectono-magmatic evolution of southern Arunta region discussed. Crystallisation age of an upper greenschist to amphibolite facies metarhyodacite. Hf analyses detailed.|1650 +/- 4 Ma (Hollis et al., 2013).||||Metamorphosed felsic, intermediate and mafic volcanics, including silicified, cryptocrystalline, porphyritic andesite; dacite; basaltic andesite; basalt; and dolerite.|13-JAN-17
42366|Walungurru Volcanics|69003|5|Briefly described|p32|Paleoproterozoic|Paleoproterozoic||c.1650 Ma.|||Overlies the Ininti Granite.|Wide range of felsic, intermediate and mafic compositions; overall calc-alkaline affinity.|
42366|Walungurru Volcanics|69031|5|Briefly described|p4, p6, p7|Statherian|Statherian|Warumpi Province, Arunta Orogen.|1650 +/- 4 Ma (Kirkland et al., 2009).|||Is intruded by Ininti Granite.|A calc-alkaline succession of volcanic and volcaniclastic rocks including metabasalt, metarhyolite and metarhyodacite.|
42366|Walungurru Volcanics|69417|6|Mentioned|p2:5|Statherian|Statherian|Kintore Region, Warumpi Province.||||||12-JUL-16
42366|Walungurru Volcanics|69428|5|Briefly described|p13:2-3, 12-13, 15|Paleoproterozoic|Paleoproterozoic|Close et al. (in prep). Kintore Domain, Warumpi Province. Crops out in the Kintore Range. Estimated at over 2000m thick. Various lithologies are described and three scenarios for magma formation discussed. A genetic relationship with Ilpilli Dolerite was suggested. Not directly dated: this 1650 Ma SHRIMP U-Pb zircon age is from a WA rhyodacite interpreted to belong to the Walungurru Volcanics.|1650 +/- 4 Ma (Kirkland et al., 2009).|||Overlies Tinki Granite. Is overlain unconformably by Heavitree Quartzite.|A succession of undeformed felsic, intermediate and mafic volcanics, with minor intervals of tuffaceous claystone, sandstone and mudstone.|12-JUL-16
42366|Walungurru Volcanics|69933|5|Briefly described|v, p1, p20-22, p39|Orosirian|Orosirian|Petrography, zircon characteristics, SHRIMP analyses and results are provided.|ca 1846 Ma (Maximum extrusion)||||Fine- to medium-grained dacitic volcanic rock, locally amygdaloidal, pale green in colour.|
42366|Walungurru Volcanics|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dacite, andesite|
42366|Walungurru Volcanics|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1650+/-4 Ma (crystallisation: U-Pb zircon).||||Metarhyodacite.|
42366|Walungurru Volcanics|71810|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Warumpi Province, Arunta Orogen, North Australian Craton.|c.1650 Ma.||||Metadacite and metarhyodacite; may include intermediate to mafic metavolcanic rocks.|
42366|Walungurru Volcanics|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Warumpi Province, Arunta Orogen.|||||Metadacite and metarhyodacite; may include intermediate to mafic metavolcanic rocks.|
42366|Walungurru Volcanics|72360|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological province: Warumpi Province. Of Kintore Domain.|||||Felsic: porphyritic andesite, dacite; local epidote-chlorite, carbonate, sericite, quartz alteration. Mafic: basalt, microdolerite, basaltic andesite, andesite, microdiorite, minor dolerite; local epidote-chlorite-sericite-quartz alteration.|09-SEP-19
41856|Waluwiya Suite|60674|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Warumpi Province.||||||07-NOV-08
41856|Waluwiya Suite|61387|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes undifferentiated rocks (high magnetic intensity) and charnockite of variable magnetic intensity.  In the Arunta region.||||||07-NOV-08
41856|Waluwiya Suite|61518|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Charnockite, granodiorite, migmatite, diorite. Geological Province: Yaya Domain.||||||07-NOV-08
41856|Waluwiya Suite|61519|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Warumpi Province||||||07-NOV-08
41856|Waluwiya Suite|61660|5|Briefly described|p18. |Proterozoic|Proterozoic|Crops out throughout the Yaya Domain. Has strong geochemical affinity with Kakalyi Gneiss.|||||Granodiorite and charnockite.|
41856|Waluwiya Suite|64580|4|Described|map legend|Paleoproterozoic|Devonian|||||||
41856|Waluwiya Suite|65329|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Shown as older than Andrew Young Igneous Complex, younger than Carrington Suite. Charnockite; high granitic magnetic response||||||
41856|Waluwiya Suite|65330|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Shown as older than Andrew Young Igneous Complex, younger than Carrington Suite. Charnockite; high granitic magnetic response||||||
41856|Waluwiya Suite|65358|6|Mentioned|p12|||Felsic. Intrudes Yaya Domain, Warumpi Province.||||||
41856|Waluwiya Suite|67565|2|Defined|p62, p19-21, p6 Table 1, p14, p32, p60.|Statherian|Statherian|New name, after Waluwiya Outstation. Previously within undifferentiated Arunta Complex (Ranford, 1969). Yaya Domain, Warumpi Province. Geochemistry is discussed briefly.|||Includes Russell and Talyi-Talyi Charnockites; Tjungkuba and Larrie Granodiorites, and Kakalyi Gneiss.|Intrudes Yaya Metamorphic Complex and Papunya Igneous Complex. Is intruded by Ehrenberg and Gunbarrel Granites and Ilpili Dolerite.|An extensive suite of variably deformed charnockite with plagioclase phenocrysts, foliated and locally migmatitic hornblende-biotite granodiorite locally containing metamorphic garnet, with lesser granite.|01-DEC-15
41856|Waluwiya Suite|68832|5|Briefly described|p12||||||Includes Talyi-Talyi Charnockite.|||
41856|Waluwiya Suite|69428|5|Briefly described|p8/11/2016 13:03|Paleoproterozoic|Paleoproterozoic|Scrimgeour et al. (2005). Yaya Domain, Warumpi Province.|1640-1630 Ma.||Larrie, Tjungkuba Granodiorites; Kakalyi Gneiss; Talyi-Talyi, Russell Charnockites.||Geochemically homogeneous, extensive Suite of variably deformed charnockite and granodiorite.|12-JUL-16
41856|Waluwiya Suite|70826|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|||||||
41856|Waluwiya Suite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||diorite, granodiorite|
41856|Waluwiya Suite|71810|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Warumpi Province, Arunta Orogen, North Australian Craton.|||||Foliated hornblende metagranodiorite to quartz metadiorite; may include two-pyroxene metagranite or migmatitic felsic rocks.|
41856|Waluwiya Suite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Warumpi Province, Arunta Orogen.|||||Foliated hornblende metagranodiorite to quartz metadiorite; may include two-pyroxene metagranite or migmatitc felsic rocks.|
41856|Waluwiya Suite|72360|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological province: Warumpi Province. Of Yaya domain.|||||Charnockite; variably migmatitic fine grained, equigranular to weakly porphyritic biotite, hornblende granodiorite; pervasively retrogressed charnockite and granodiorite; abundant epidote retrogression and quartz-epidote veining.|09-SEP-19
31768|Wandarrie Granite|23569|4|Described|p5 Tb. 1|Archean|Archean|Of the Narryer Terrane.   Coarse-grained, equigranular, leucocratic monzogranite.||||||07-NOV-08
31768|Wandarrie Granite|23574|5|Briefly described|Map Legend|Archean|Archean|Overlying Unit Yallalong Granite.||||||07-NOV-08
31768|Wandarrie Granite|23576|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Yallalong Granite.||||||07-NOV-08
31768|Wandarrie Granite|23577|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Yallalong Granite.||||||07-NOV-08
31768|Wandarrie Granite|24114|5|Briefly described|p5 Fig.4|Archean|Archean|Geological Province: Yilgarn Craton. Age: c. 2735 Ma.||||||07-NOV-08
31768|Wandarrie Granite|43835|5|Briefly described|Map Legend|Archean|Archean|Age about 2735Ma.||||||07-NOV-08
31768|Wandarrie Granite|73526|5|Briefly described|p2 Fig.1, p3|Neoarchean|Neoarchean|Narryer Terrane, westernmost. See also Wandarrie granite p4 Tb.1, age of 2735+/-9 Ma.|c. 2735 Ma||||Granitic intrusion.|
34367|Wandarry Supersequence|22682|5|Briefly described|Fig5,p10|Orosirian|Orosirian|1906-1862 Ma. Ashburton Province||||||
36477|Wandiwarra Member|23529|5|Briefly described|p10|Paleoproterozoic|Paleoproterozoic|Formerly Wandiwarra Formation.  Parent: Chiall Formation.  Max. thickness: ~500m.   Geological Province: Earaheedy Basin||||||07-NOV-08
36477|Wandiwarra Member|23581|5|Briefly described|Map legend||Paleoproterozoic|Of the Chiall Formation in the Earaheedy Group in the Earaheedy Basin||||||07-NOV-08
36477|Wandiwarra Member|23589|4|Described|p28|||Previously Wandiwarra Formation. Of Chiall Formation. Geological Province: Earaheedy Basin.||||||25-NOV-13
36477|Wandiwarra Member|23611|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|See also page 33 Appendix 1.  Of Chiall Formation. Geological Province: Earaheedy Basin.||||||07-NOV-08
36477|Wandiwarra Member|24017|4|Described|p18|Paleoproterozoic|Paleoproterozoic|Formerly Wandiwarra Formation.  Of the Chiall Formation.  Geological Province: Earaheedy Basin.||||||07-NOV-08
36477|Wandiwarra Member|24018|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Chiall Formation, Earaheedy Group.  Geological Province: Earaheedy Basin.||||||07-NOV-08
36477|Wandiwarra Member|24578|5|Briefly described|p784|Paleoproterozoic|Paleoproterozoic|Of the Chiall Formation. Geological Province: Earaheedy Basin||||||07-NOV-08
36477|Wandiwarra Member|50188|5|Briefly described|p4 Fig. 2, p6, p8|||Of Chiall Formation. Formerly Wandiwarra Formation now downgraded to member status. Overlies Karri Karri Member. Geol.Prov: Earaheedy Basin. Lithic wacke and quartz wacke.||||||16-JUL-08
36477|Wandiwarra Member|50195|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Chiall Formation.  Age: <2048Ma.  Geological Province: Earaheedy Basin.||||||07-NOV-08
36477|Wandiwarra Member|50222|5|Briefly described|p320 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Chiall Formation (Miningarra Sungroup, Earaheedy Group).   Glauconite.  Geological Province: Earaheedy Basin.||||||07-NOV-08
36477|Wandiwarra Member|50223|5|Briefly described|p345 Fig. 2, p346|Paleoproterozoic|Paleoproterozoic|Of the Chiall Formation (Miningarra Subgroup, Earaheedy group).  Composed of shale, siltstone and fine to coarse quartz wacke and arenite.  Geological Province: Earaheedy Basin.  See also p351.||||||07-NOV-08
36477|Wandiwarra Member|50626|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Chiall Formation (Earaheedy Group).  Sandstone, siltstone and shale.  Geological Province: Earaheedy Basin.||||||07-NOV-08
36477|Wandiwarra Member|63866|5|Briefly described|p167|Statherian|Statherian||1688 +/- 72 Ma (K-Ar, Horwitz, 1975 Ma)|Yelma Formation||||
36477|Wandiwarra Member|64284|5|Briefly described|p60 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of Chiall Formation (Minningarra Subgroup). Replaces part of Wandiwarra Formation and Princess Ranges Quartzite. Geological Province: Earaheedy Basin||||||07-FEB-11
36477|Wandiwarra Member|64772|5|Briefly described|p12, p10 Fig. 5|Paleoproterozoic|Paleoproterozoic|Superseded "Wandiwarra Formation". Of Chiall Formation. See also p25 Fig.11, p26 Fig.13, p33 Fig.21, p39 Fig.25, p75 App.4 Tb.4.3|||||Shale, sandstone|25-NOV-13
36477|Wandiwarra Member|65264|5|Briefly described|p27|Paleoproterozoic|Paleoproterozoic|Of Chiall Formation (Mooloogool Subgroup). Overlies Karri Karri Member. Geological province: Earaheedy Basin. Comprises sandstone and shale.||||||07-FEB-11
36477|Wandiwarra Member|65472|5|Briefly described|p3 Fig.2|Paleoproterozoic|Paleoproterozoic|Age: from Fig.2, after Pirajno et al. Glauconite. Earaheedy Basin. |1.68 Ma whole rock K-Ar|Chiall Formation||||24-SEP-15
36477|Wandiwarra Member|65692|6|Mentioned|p56|||||Chiall Formation.||||
36477|Wandiwarra Member|66427|5|Briefly described|p44 Tb.2, p46-48, p63-67, p73|||Here replaces Wandiwarra Formation (see references to that unit: p46 Fig.4, p48, p63). Recognised as part of a single depositional episode.|1685 +/- 35 Ma (K-Ar; Horwitz, 1975).|Unit in Chiall Formation.|||Consists dominantly of siltstone and shale, with scattered intercalations of sandstone.|
36477|Wandiwarra Member|69003|5|Briefly described|p14 Fig.18|||Earaheedy Basin.||Chiall Formation.||Unconformably overlies Windidda Member (Frere Formation).||
36477|Wandiwarra Member|69152|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin||Chiall Formation|||Siltstone, sandstone, minor limestone; commonly glauconitic; rippled to cross-bedded, local hummocky cross-stratification; common ball-and-pillow structures.|07-AUG-15
36477|Wandiwarra Member|69313|5|Briefly described|p25 Fig.4.3|||||Chiall Formation||Overlies the Karri Karri Member and the Windidda Member. Overlain by the Princess Ranges Member.|Siltstone and fine sandstone interbedded with coarser sandstone.|
36477|Wandiwarra Member|69596|6|Mentioned|p10|||Earaheedy Basin.||Chiall Formation.||||
36477|Wandiwarra Member|70153|5|Briefly described|100k_geologyp10_lut.csv|Paleoproterozoic|Paleoproterozoic|||Chiall Formation|||Siltstone, sandstone, minor limestone; commonly glauconitic; rippled to cross-bedded, local hummocky cross-stratification; common ball-and-pillow structures.|
36477|Wandiwarra Member|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, shale, sandstone|
36477|Wandiwarra Member|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen. Of Earaheedy Basin. See 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.||Unit of Chiall Formation.|||Siltstone, sandstone, minor limestone; commonly glauconitic; rippled to cross-bedded, local hummocky cross-stratification; common ball-and-pillow structures|
79007|Wangata Monzogranite|70226|5|Briefly described|Map legend.|Neoarchean|Neoarchean|Yilgarn Craton.||Walganna Suite|||Coarse-grained, undeformed monzogranite with distinctive igneous layering defined by gradational variation in the modal abundance of biotite and K-feldspar (0.5 to 3 m scale); K-feldspar up to 30 mm long; metamorphosed.|16-DEC-15
79007|Wangata Monzogranite|70796|5|Briefly described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton. See also 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, Yalgoo100_2241_stratig.pdf.|ca 2626 Ma (inferred)|Walganna Suite|||Coarsegrained, undeformed monzogranite with distinctive igneous layering defined by gradational variation in the modal abundance of biotite and Kfeldspar (0.5 to 3 m scale); Kfeldspar up to 30 mm long; metamorphosed|
79007|Wangata Monzogranite|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.|2626 Ma|Unit of Walganna Suite.|||Coarse-grained, undeformed monzogranite with distinctive igneous layering defined by gradational variation in the modal abundance of biotite and K-feldspar (0.5 to 3 m scale); K-feldspar up to 30 mm long; metamorphosed|
73851|Wangee Formation|24391|4|Described|p8-4 Fig.2|Archean|Archean|Of Point Samson Group. Black-white laminated chert, massive black chert and felsic hyaloclastite with black chert dykes. Geological Province: Pilbara Block.||||||07-NOV-08
31146|Wangina Sandstone|43495|5|Briefly described|11-16|||||||||
79351|Wangine Monzogranite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|3010-2600 Ma (inferred)||||Leucocratic, medium-grained, biotite-bearing monzogranite|
83880|Wanjarri Granite|69414|6|Mentioned|p88|Archean|Archean|Agnew-Wiluna Greenstone belt, Kalgoorlie Terrane, Yilgarn Craton.||||||
73256|Wankanki Supersuite|63864|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Rocks consist of; mylonitic leucocratic granite, weakly to strongly foliated porphyritic metamonzogranite, orthopyr-clinopyr-biotite granite, metaleucogranite and mylonite. For more info see map legend.||||||05-AUG-08
73256|Wankanki Supersuite|64722|5|Briefly described|Fig. 2 p3-6, p17|Ectasian|Ectasian|Western Musgrave Orogen. Calc-alkaline I-type rocks with a magmatic arc signature.|U-Pb ages of 1340-1300 Ma.||||Felsic gneiss and granitic rocks.|11-APR-12
73256|Wankanki Supersuite|65135|4|Described|p1, p5, p6 Fig.4, pp10-13, p18|Ectasian|Ectasian|Intrudes Wirku Metamorphics. In lower strain zones, typically porphyritic I-type granodiorites and monzogranites. Strongly deformed and metamorphosed to granulite facies. Migmatised in most leucocratic granites. Geochemically similar granulites in the Cavenagh Range interpreted to represent volcanic and volcaniclastic equivalents (Smithies et al., 2008). Crystallisation ages range from ~1336-1293 Ma, and mostly between 1326-1312 Ma (White et al., 1999; Kirkland et al., 2008). Includes xenoliths of Wirku Metamorphics.||||||
73256|Wankanki Supersuite|65693|6|Mentioned|p3 Fig.1.|||||||||
73256|Wankanki Supersuite|65833|4|Described|p1. p5, p6 Fig.4, p11, p12 Fig.8, p13|Ectasian|Ectasian|Howard et al.(2007). Porphyritic granodiorites and monzogranites containing clinopyroxene, orthopyroxene and late hornblende. Typically strongly deformed and sometimes migmatised. Protolith crystallisation age range: 1336-1293 Ma; most within c.1326-1312 Ma. Silica range 58.95-76.76 wt%. Metaluminous, calc-alkaline I-types; volcanic arc granites. Product of Mount West Orogeny. Intrudes Wirku Metamorphics and locally contains xenoliths and rafts of that unit.||||||
73256|Wankanki Supersuite|65898|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province. 2 unnamed units shown. Weakly to strongly foliated, porphyritic metamonzogranite; interleaved orthopyroxene-clinopyroxene-biotite gneissic granite and fine to medium grained schleric opx(-hornblende) leucogranite.||||||
73256|Wankanki Supersuite|65906|5|Briefly described|p3, p5|Mesoproterozoic|Mesoproterozoic|Voluminous felsic intrusive magmatism: granites formed during the 1336-1293 Ma Mount West Orogen, associated with granulite facies metamorphism and migmatisation.||||||
73256|Wankanki Supersuite|65907|5|Briefly described|pp3-5, p9 .|||These high-grade intrusives incorporate rafts of Wirku Metamorphics in the west of the Musgrave Block. Probable continental arc setting.|c.1336-1293 Ma.||||Granites.|
73256|Wankanki Supersuite|66241|5|Briefly described|p28.|Ectasian|Ectasian||1336 - 1203 Ma.|||Intrudes Wirku Metamorphics.||
73256|Wankanki Supersuite|66256|5|Briefly described|p4 Fig.3, p6, p8, p10-11, see comments|Ectasian|Ectasian|Of Howard et al. (2007). Granitic and volcanic rocks produced during Most West Orogeny crustal event. Crystallization age range (SHRIMP); most occur between c. 1326 and 1312 Ma. Interpreted to have protoliths of sedimentary and lesser volcaniclastic and volcanic origin. In west Musgrave Province. All rocks have been recrystallized at granulite facies. Granite geochemistry provided (whole-rock geochemical, Nd and Hf isotopic analyses). SHRIMP results for metamorphic age: Mamutjarra Zone 1127+/-9 to 1185+/-20 Ma; Tjuni Purlka Tectonic Zone 1178+/-21 to 1233+/-21 Ma. See also p17-29, p32-34, p38-39, p44-46, p53-54 App.1, p68-70 App.3, p71 App.4.|1345 +/- 7 Ma to 1293 +/- 9 Ma.|||Veins and sheets of Tjuni Purlka suite cut and engulf rocks of Wankanki Supersuite.|Granitic and volcanic rocks; metamorphosed to granulite facies.|11-JAN-17
73256|Wankanki Supersuite|66280|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Map shows four unnamed units: foliated, porphyritic monzogranite; composite volcanic-sedimentary gneiss; composite felsic volcanic-granulite gneiss; composite felsic volcanic-psammite gneiss.||||||
73256|Wankanki Supersuite|66281|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province.|1336-1293 Ma.||||Hypersthene-biotite granodiorite to monzogranite; enderbite to charnockite; migmatitic gneiss; foliated meta-syenogranites.|
73256|Wankanki Supersuite|66282|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Metagranite and gneiss; metafelsic volcanics mixed with interlayered psammite and pelite.|1336 - 1293 Ma.||||A variety of lithologies including gneissic granite, gneisses, metasyenogranite, metamonzogranite, mylonite derived from granite or gneiss, composite gneisses of volcanic/volcaniclastic units and acid/intermediate granulite.|
73256|Wankanki Supersuite|66284|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Comprises two separately-mapped but un-named units.|1336 - 1293 Ma.||||Composite gneiss with felsic volcanic/volcaniclastic units interlayered with acid to intermediate granulite; composite gneiss with felsic volcanic/volcaniclastic units interlayered with psammite, garnetiferous pelite, and rare calc-silicate rocks.|
73256|Wankanki Supersuite|67128|5|Briefly described|p5 Fig.3, p6-8, p15|||Howard et al. (2009). Tjuni Purlka Tectonic Zone, western Musgrave Province. Forms part of the Ramarama Basin. Felsic, arc-signature intrusions and volcanism associated with the c.1345-1293 Ma Mount West Orogeny.|c.1345-1293 Ma.|||Is overlain unconformably by MacDougall Formation.|Moderately foliated porphyritic granites, layered felsic gneisses showing incipient to adavnced migmatization. Fine-grained gneisses from volcanic protoliths.|
73256|Wankanki Supersuite|67244|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Mapped as three separate but un-named sub-units.|||||Hypersthene-biotite granodiorite to monzogranite; enderbite to charnockite; moderately foliated to gneissic; weakly to strongly foliated biotite metasyenogranite, typically with abundant microcline.|
73256|Wankanki Supersuite|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Mapped as 13 separate but un-named units.|1345 - 1293 Ma.||||Foliated to gneissic hypersthene-biotite granodiorite to monzogranite, enderbite to charnockite; hornblende leucosyenogranite; migmatitic gneiss; gneissic granite; metasyenogranite; mylonite; metafelsic volcanics; composite gneisses.|
73256|Wankanki Supersuite|67375|3|Fully described|p6, p13, pp21-22, pp24-26, pp124-148.|Mesoproterozoic|Mesoproterozoic|West Musgrave Province. Name derived from local (Pitjantjatjara) name for Mount West ('Puli Wankanki'), the type locality for this Supersuite. I-type. Metaluminous and calcic to calc-alkalic. Strongly deformed granites, metamorphosed up to granulite facies. Tectonic setting possibly a continental arc. Volcanic units are interlayered with, and contributed detritus to, the Wirku Metamorphics; xenoliths and rafts of this latter Group locally occur within the granites.|1347 +/- 7 to 1293 +/- 9 Ma (mostly 1326-1312 Ma).|||Intrudes and engulfs Wirku Metamorphics. Is intruded by granites of the Warakurna Supersuite. Is overlain unconformably by MacDougall Formation of Kunmarnara Group.|Calc-alkaline granites, deformed and migmatized; typically within the compositional range of quartz monzonite to syenogranite, with granodiorites and monzogranites dominant; generally leucocratic, with up to 12% mafic minerals; locally porphyritic.|
73256|Wankanki Supersuite|67553|4|Described|p8-9,11-12,16-17,19,22-23,25-27|Ectasian|Ectasian|Geological province: Musgrave Province, North Australian Craton. Calc-alkaline granites, dominant within the Mamutjarra Zone. Produced by Mount West Orogeny, affected by Musgrave Orogeny. Average mantle extraction age of basement components 2040-1840 Ma. Calc-alkaline magmatism at 1318+\-19 Ma (GSWA 194765). Large-scale folding related to SE-NW compression at ?1293-M1220 Ma (post tectonic intrusion of Pitjantjatjara intrusions across NE trending folds; GSWA 184146 and 185610). Strongly deformed, and metamorphosed to granulite facies. Includes xenoliths and rafts of Wirku Metamorphics within granites of Wankanki Supersuite. The Wankanki Supersuite may reflect final stage in Proterozoic amalgamation of central Australia (Giles et al., 2004; Betts and Giles, 2006; Smithies et al., 2010), ending before main onset of Musgrave Orogeny, with a collisional event that produced regional NE-trending folds. See also p31,59,73,77-78.|1345-1293 Ma||||Metaluminous, calc-alkaline, I-type rocks including a leucogranitic dyke.|06-AUG-19
73256|Wankanki Supersuite|67888|5|Briefly described|p61|Mesoproterozoic|Mesoproterozoic||1345-1293 Ma||||Calcalkaline volcanic and intrusive rocks.|
73256|Wankanki Supersuite|68077|5|Briefly described|p1, p3-5, p16-17, p19, p30, p32-36, p38|Mesoproterozoic|Mesoproterozoic|See also p42. Calc-alkaline granites were produced by the Mount West Orogeny. Rocks are compositionally indistinguishable from those of the older Papulankutja Supersuite. Isotopic composition (Lu-Hf and Sm-Nd) and evolution tabulated and discussed in detail.|1345-1293 Ma|||Interleaved with Wirku Metamorphics.|Metaluminous, calcic to calc-alkaline granodiorites, monzogranites, granite, metasiltstone, metasandstone.|07-SEP-17
73256|Wankanki Supersuite|68100|4|Described|p1, 2, 3,4,7-9,13-16,19, 4-28,31,33-p36|Mesoproterozoic|Mesoproterozoic|Together with the Wirku Metamorphics forms the Ramarama Basin. Often interlayered and intruded with Wirku Metamorphics.All rocks have undergone granulite facies metamorphism. Includes volcanogenic gneisses.|1326-1293 Ma, 1334+/-6 Ma Max deposition|||Porphyritic granites intrude Wirku Metamorphics. Gneisses with volcanic protolith interlayered with Wirku Metamorphics.|Calc-alkaline volcanic and intrusive rocks. Mafic and felsic magmatic rocks, foliated I-type porphyritic granites, layered felsic gneisses showing incipient to advanced migmatization.Arkosic metasandstone.|
73256|Wankanki Supersuite|68995|5|Briefly described|p2, p48, p51 Tb. 4|Ectasian|Ectasian|Musgrave Province, deposited during the Mount West Orogeny. Ages derived from studies by Gray, 1971, Sun et al, 1996, White et al, 1999 and Bodorkos and Wingate, 2008. Ages are concentrated between 1326-1312 Ma. |1345-1293 Ma (crystallization ages)||||Metaluminous, calcic to calc-alkaline granodiorites and monzogranites.|
73256|Wankanki Supersuite|68996|5|Briefly described|p2-3, 4, 24, 27-29, 33, 35-46, 49, 54|Mesoproterozoic|Mesoproterozoic|Mount West Orogeny granites. Age is of magmatism. Density ranging from 2.60-3.09 g/cm^3,|1345-1293 Ma||||Porphyritic granodiorites and monzogranites, typically with a significant mafic mineral component of cpx, opx and hornblende; granitic gneiss.|
73256|Wankanki Supersuite|69003|5|Briefly described|p4, p37-39, p42, p45|Mesoproterozoic|Mesoproterozoic|W Musgrave Province, Paterson Orogen. Associated with the Mount West Orogeny. Continental margin arc geochemistry and istopic compositions.|1345-1293 Ma.||||Voluminous felsic magmatism, both plutonic and volcano-sedimentary rocks.|
73256|Wankanki Supersuite|69009|6|Mentioned|Map Legend|||Musgrave Province. Only shown on Interpreted Bedrock Geology diagram (instead of Pitjantjatjara Supersuite).|||||Comprises gneissic granite and leucogranite.|28-MAY-15
73256|Wankanki Supersuite|69091|4|Described|p52 Fig.4.1, p53, see comments|Mesoproterozoic|Mesoproterozoic|Of west Musgrave Province. Dominates Mamutjarra Zone. Formed during Mount West Orogeny. Age analysis of fine-grained, unfoliated leucogranitic dyke has igneous crystallisation age of 1318 +/- 9 Ma (GSWA 194765, Kirkland et al., in prep); U-Pb SHRIMP dating. On tectonic discrimination diagrams these rocks consistently fall within field for volcanic-arc granites, and in this respect they differ from all other granites in west Musgrave Province. See also p54 Fig.4.2, p55 Fig.4.3, p56, p59 Fig.4.6, p61-67, p82, p86, p103 Fig.5.6, p117 Fig.5.15, p131 incl. Fig.6.1, p132, p137-139 Figs.6.4-6.6, p141 Fig.6.8, p142, p181, p183, p190.|c. 1345-1293 Ma, most between c. 1326 - c. 1312 Ma|||Intrudes sedimentary protoliths to the Wirku Metamorphics; dyke cuts Papulankutja Supersuite; unconformably overlain by Kunmarnara Group.|Felsic units; metaluminous, calc-alkaline, I-type granites; strongly deformed and metamorphosed up to granulite facies; porphyritic granodiorites and monzogranites, often with a significant mafic mineral component, including cpx, opx and hornblende.|
73256|Wankanki Supersuite|69153|5|Briefly described|GEOL_LUT_CSV files;GEOCHRON/194637.1.pdf|Mesoproterozoic|Mesoproterozoic|Paterson Orogen, Musgrave Province. Age mentioned in GEOCHRON/194764.1.pdf and other Geochron records.|1345-1293 Ma (Smithies et al., 2010)|||is intruded by Warakurna Supersuite|Meta-sedimentary siliciclastic: psammite and pelite, interlayered; meta-igneous felsic: granite, granodiorite, monzogranite, enderbite, charnockite; migmatitic gneiss derived from granodiorite, monzogranite, sedimentary and volcaniclastic protoliths|
73256|Wankanki Supersuite|69436|6|Mentioned|p21:2||||1345-1293 Ma.|||||12-JUL-16
73256|Wankanki Supersuite|69554|6|Mentioned|p139|||Western Musgrave Province.|||||Orthogneisses.|
73256|Wankanki Supersuite|69655|5|Briefly described|p3, p5-p7, p9, p77-p78|Ectasian|Ectasian|Musgrave Province. Mount West Orogeny. Ages cluster between c. 1326 and 1312 Ma.|c. 1345-1293 Ma||||Metaluminous, calcic to calc-alkaline granodiorites and monzogranites with strong compositional similarities to the Andean continental arc.|
73256|Wankanki Supersuite|69729|5|Briefly described|p66 Fig.1, p67-75, p77, p85, p88, p90|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Formed during the Mount West Orogeny. Probably continental arc magmatism. Geochemistry plots.|1345-1293 Ma.||||Calc-alkaline granites, typically strongly deformed and metamorphosed up to granulite facies. Mainly monzogranite ansd syenogranite; rare tonalite and granodiorite. Gabbroic enclaves are very rare.|
73256|Wankanki Supersuite|70083|6|Mentioned|p206|||Western Fregon Subdomain, Musgrave Inlier. Associated with the 1345-1293 Ma Mount West Orogeny. Characterised by high-grade metamorphism and calc-alkaline magmatism.|1345-1293 Ma.||||Granites; calc-alkaline magmatism associated with layer-parallel migmatitic fabric and F1 folding.|
73256|Wankanki Supersuite|70084|4|Described|p219-221,223-225,227-228|Ectasian|Ectasian|Geological province: Musgrave Province, Paterson Orogen. Has close compositional similarity to Phanerozoic andean continental arc magmas (Giles et al., 2004; Betts and Giles, 2006; Smithies et al., 2011; Howard et al., 2011; Kirkland et al., 2013a) associated with Mount West Orogeny and coeval with Wirku Metamorphics, and Recherche Supersuite and Fraser Range Metamorphics in the Albany-Fraser Orogen. Emplacement age between c. 1326 and 1312 Ma (Howard et al., 2011). Preserved as banded paragneiss rafts in granite. Detrital zircon age spectra with peaks around 1575, 1560, 1500, 1410 and 1360 Ma, and rare peaks around 2630 and 2710 Ma (Latitude Hills, SE of W Musgrave Province; Evins et al., 2012). Lies within a single, narrow, Nd and Hf-isotopic evolution band with TDM2 values within a range of 2.2-1.6 Ga, together with the Pitjantjatjara, Papulankutja and Warlawurru supersuites, reflecting reworking of juvenile crust between ca. 2.0 and 1.6 Ga (Kirkland et al., 2013a).|c. 1300 Ma||||Granites, typically metaluminous and calcic to calc-alkalic, with silica-rich rocks and almost completely lacking grabbroic members.|09-JUN-20
73256|Wankanki Supersuite|70090|6|Mentioned|p456|||Geological province: Musgrave Province.||||||
73256|Wankanki Supersuite|70182|6|Mentioned|p44 Fig.29|||Musgrave Province.||||||
73256|Wankanki Supersuite|70619|6|Mentioned|map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Shown only on small interpreted bedrock geology map.|||||Gneissic granite and leucogranite.|03-JUN-16
73256|Wankanki Supersuite|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|SHRIMP dates from samples (183587.1.pdf, 184158.1.pdf)|1303 Ma +/- 10 Ma 1351 Ma +/-8 Ma (SHRIMP)|||Intruded by Warakurna Supersuite|Hypersthene-biotite granodiorite to monzogranite; enderbite-charnockite, monzogranite to granodiorite. Porphyritic metamonzogranite, migmatitic gneiss. Gneissic granite, metasyenogranite, leucosyenogranite, composite gneiss.|
73256|Wankanki Supersuite|70748|6|Mentioned|p56|||||||||
73256|Wankanki Supersuite|70763|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province.|||||Gneissic granite and leucogranite.|
73256|Wankanki Supersuite|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Formed during Mount West Orogeny (Howard et al., 2007). Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma); Musgrave Orogeny (1220-1150 Ma); Mount West Orogeny (1345-1293 Ma). Sample GSWA 180867 (quartz monzonite) yielded an interpreted (weighted mean 207Pb*/206Pb*) magmatic crystallisation age of 1324+\-7 Ma, and metamorphic zircon rim growth at 1191+\-12 Ma. Sample GSWA 183492 (K-spar porphyritic granite) yielded an interpreted (weighted mean 207Pb*/206Pb*) magmatic crystallisation age of 1322+\-6 Ma, and metamorphic zircon rim growth at 1182+\-15 Ma. Sample GSWA 183496 (orthogneiss) yielded an interpreted (weighted mean 207Pb*/206Pb*) magmatic crystallisation age of 1321+\-7 Ma for the granitic protolith, and metamorphism at 1178+\-21 Ma. Sample GSWA 183587 (magmatic leucogranite) yielded an interpreted (weighted mean 207Pb*/206Pb*) best estimate age of crystallisation at 1351+\-8 Ma, and metamorphic events based on zircon rims and overgrowth at 1206+\-10 Ma, 1066+\-9 Ma and 1024+\-24 Ma. Sample GSWA 183726 (leucogranitic gneiss) yielded an interpreted (weighted mean 207Pb*/206Pb*) magmatic crystallisation age of 1314+\-8 Ma, and high-grade metamorphism and migmatisation dated at 1222+\-9 Ma and 1191+\-9 Ma. Sample GSWA 184158 (metamonzogranite) yielded an interpreted (207Pb*/206Pb*) igneous crystallisation date of 1303+\-10 Ma. Sample GSWA 185581 ( biotite monzogranite) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) magmatic crystallisation date of 1312+\-7 Ma. Sample GSWA 185606 (biotite leucogranite) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) magmatic crystallisation age of 1324+\-7 Ma. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 500k_interpgeop_lut.csv, 2_5m_interpgeop15_lut.csv.|1345-1293 Ma (inferred)|||Intruded by Warakurna Supersuite. Intrudes into Wirku Metamorphics.|Hypersthene-biotite (in part charnockitic) granodiorite to monzogranite, metamonzogranite, mignatitic gneiss, gneissic granite, leucosyenogranite, composite gneiss with felsic volcanic and volcaniclastics units.|
73256|Wankanki Supersuite|70826|6|Mentioned|p10|Mesoproterozoic|Mesoproterozoic|Mount West Orogeny.|1345-1293 Ma (Age of Orogeny)|||||
73256|Wankanki Supersuite|70831|5|Briefly described|p2-p3, p5, p26|Ectasian|Ectasian|West Musgrave Province. Interpreted to have formed in a continental arc setting during the Mount West Orogeny.|c. 1345-1293 Ma|||Intrudes the Papulankutja Supersuite.|Metaluminious, calc-alkaline, I-type magamtic rocks.|
73256|Wankanki Supersuite|70839|5|Briefly described|p326-327,334,336,339|Ectasian|Ectasian|Geological province: Musgrave Province. Voluminous calc-alkaline plutonism and associated clastic and volcaniclastic rocks associated with 1345-1293 Ma Mount West Orogeny, reflecting the final amalgmation of the combined North and West Australian Craton with South Australian Craton (Howard et al., 2015).|1345-1293 Ma|||||
73256|Wankanki Supersuite|71088|5|Briefly described|p4-p5, p25|||West Musgrave Province. Intruded during the Mount West Orogeny.|c. 1345-1293 Ma||||Calc-alkaline plutonic rocks.|
73256|Wankanki Supersuite|71169|5|Briefly described|p80|Ectasian|Ectasian|Western Musgrave Province. Deposited during the Mount West Orogeny. May have been deposited in a continental arc or contains an inherited arc signature.|1345-1295 Ma||||Arc-like felsic intrusive rocks.|
73256|Wankanki Supersuite|71170|5|Briefly described|p5-p6, p9|Mesoproterozoic|Mesoproterozoic|West Musgrave Orogen. Emplaced during the Mount West Orogeny. Compositionally similar to Phanerozoic granites of the Andes and therefore could be linked to final accretion during amalgamation of South, North and West Australian cratons.|1345-1293 Ma||||Metaluminous, calc-alkaline granodiorites and monzogranites.|
73256|Wankanki Supersuite|71210|5|Briefly described|p3-p5, p7, p21, p23|||Musgrave Province. Defined by Howard et al., 2007b. See also p51, p53, p66-p67, p78-p81, p97, p99, p113.|1345-1293 Ma||||Granulite facies calcic to calc-alkaline, metaluminous I type granitoid gneisses and associated volcanic rocks.|
73256|Wankanki Supersuite|71211|5|Briefly described|p6, p7 fig 1.4, p24 fig 2.1|||Musgrave Province.  Alternate crystallisation ages of 1326-1312 Ma have been given on p229.  Granites of this suite are metaluminous. See also p84 fig 3.1, p136 fig 4.1, p229.|1345-1293 Ma||||Calcic to calc-alkaline granodiorites and monzogranites.|
73256|Wankanki Supersuite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma); Musgrave Orogeny (1220-1150 Ma); Mount West Orogeny (1345-1293 Ma). Sample GSWA 180867 (quartz monzonite) yielded a weighted mean 207Pb/206Pb date of 1324+\-7 Ma, interpreted as the magmatic crystallisation age of the quartz monzonite; and 1191+\-12 Ma, intepreted to be age of metamorphic zircon rim growth. Sample GSWA 183492 (porphyritic granite) yielded weighted mean 207Pb/206Pb dates of 1322+\-6 and 1182+\-15 Ma, interpreted to be age of magmatic crystallisation, and metamorphic zircon growth respectively. Sample GSWA 183496 (quartz monzodiorite) yielded weighted mean 207Pb/206Pb dates of 1321+\-7 and 1178+\-21 Ma, interpreted to be age of magmatic crystallisation of igneous protolith, and metamorphism respectively. Sample GSWA 183587 (migmatitic leucogranite) yielded a weighted mean 207Pb/206Pb dates of 1351+\-8, interpreted to be best estimate age of crystallisation of leucogranite, and three subsequent metamorphism events (weight mean ages) at 1206+\-1, 1066+\-9 and 1024+\-24 Ma. Sample GSWA 184158 (metamonzogranite) yielded a weighted mean 207Pb/206Pb age of 1303+\-10 Ma, interpreted as igneous crystallisation age of monzogranite. Sample GSWA 185581 (bt monzogranite) yielded a concordia age of 1313+\-7 Ma, interpreted as magmatic crystallisation age. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|1345-1293 Ma (inferred)|||Overlain unconformably by Bentley Supergroup.|Composite gneiss: leucocratic felsic volcanic and volcaniclastics interlayered with felsic granulite, psammite and pelite; monzogranite to granodiorite mylonitic gneiss or granite; foliated biotite metasyenogranite ot porphyritic metamonzogranite.|21-APR-21
73256|Wankanki Supersuite|71321|4|Described|p5,10,35-38,63|Ectasian|Ectasian|Geological province: Musgrave Province. Restricted in the western Musgrave Province. Intruded and crystallised during Mount West Orogeny (Howard, et al., 2011a; Smithies, et al., 2009; Smithies, et al., 2011) in a volcanic arc settin with similar geochemical trends to modern arc granites. Deformed and metamorphosed at amphibolite to granulite facies during the province-wide c. 1220-1120 Ma Musgravian Orogeny (Edgoose, et al., 2004; Major and Conor, 1993; Smithies, et al., 2010). Geochemically similar to Birksgate Complex paragenisses in the Musgrave Province (strong compositional similarities to Phanerozoic granites of the Andean continental arc (Smithies, et al., 2010).|c. 1345-1293 Ma|||Near synchronous with Wirku Metamorphics.|Calcic to alkali-calcic granitoids.|
73256|Wankanki Supersuite|71322|5|Briefly described|p31|||Emplaced during the Mount West Orogeny. Dominantly igneous but contains rafts of metasediments.|c.1335-1290 Ma.|||||
73256|Wankanki Supersuite|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1312+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Foliated biotite granite, orthogneiss, granitic gneiss, migmatitic gneiss, K-ferldspar porphyritic granite, migmatitic leucogranite, quartz monzonite.|
73256|Wankanki Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Musgrave Province, Paterson Orogen. Inferred age range ~1345- 1293 Ma.|ages: 1324+/-4 Ma, 1321+/-3 Ma, 1319+/-7 Ma.||||Metagranite+ gneiss. Metamorphosed felsic volcanic rocks mixed w interlayered psammite, pelite. Interleaved orthopyroxene-clinopyroxene-biotite gneissic granite + fine- to medium-grained schlieric orthopyroxene(-hornblende)-bearing leucogranite.|
73256|Wankanki Supersuite|72059|5|Briefly described|p67|Ectasian|Ectasian|Geological province: Musgrave Province. Coeval with Recherche Supersuite. Calc-alkalic granites formed from a magmatic arc related to subduction of a Proterozoic oceanic plate (the Madura plate) along the margin of the Musgrave Province to the NE.|||||Calc-alkalic granitic rocks.|03-FEB-20
73256|Wankanki Supersuite|72094|5|Briefly described|p2, p3 Fig 2|Ectasian|Ectasian|Musgrave Province.  Granitic magmas emplaced during Mount West Orogeny (Smithies et al., 2010; Howard et al., 2011). Underwent UHT metamorphism during Musgrave Orogeny.|1345-1293 Ma||||Metagranite and gneiss|
73256|Wankanki Supersuite|72242|5|Briefly described|p27|Ectasian|Ectasian|Geological province: Musgrave Province. Associated with Mount West Orogeny.||||||
73256|Wankanki Supersuite|72443|5|Briefly described|p736-737, p747|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Produced by the Mount Westy orogeny.|1345-1293 Ma||||Metaluminous, calc-alkaline granites.|
73256|Wankanki Supersuite|72949|6|Mentioned|p40|Stenian|Stenian|Musgrave Province. Represents episodic magmatism with subduction-related, arc-type geochemistry.|c. 1.35-1.29 Ga|||||
73256|Wankanki Supersuite|73058|5|Briefly described|p760-761, p770-771, p776, p778-779|Ectasian|Ectasian|Musgrave Province, Tjuni Purlka Tectonic Zone and Mamutjarra Zone. Typically metaluminous, calcic to calc-alkaline granites. Of the Mount West Orogeny (1345-1293 Ma). Crystallisation ages are concentrated at c. 1326-1312 Ma. 1318+/-9 Ma age from an unfoliated leucogranitic dyke intruding the Papulankutja Supersuite. Hf and Nd model ages suggest mantle extraction event at c. 1900 Ma. Location in text includes p772 Fig.8-9, p773-775, p777 Fig.14.|c. 1345-1293 Ma||||Typically granodiorites and monzogranites.|
73256|Wankanki Supersuite|73084|6|Mentioned|p101, p103-104, p109|Ectasian|Ectasian|Musgrave Province.|c. 1300 Ma||||Includes calc-alkaline granites.|
73256|Wankanki Supersuite|73166|6|Mentioned|p652 Fig. 8, p656|Mesoproterozoic|Mesoproterozoic|Musgrave Province.|1345-1293 Ma|||||
73256|Wankanki Supersuite|73177|5|Briefly described|p1100|||Musgrave Province.|c.1300 Ma.|||||
73256|Wankanki Supersuite|73242|6|Mentioned|p47|Ectasian|Ectasian|Musgrave Province. Calc-alkaline felsic plutonism.|1330-1280 Ma|||||
73256|Wankanki Supersuite|73346|6|Mentioned|p2, p5|||Musgrave Province. Produced during the 1345-1293 Ma Mount West Orogeny.|||||Calc-alkaline plutonic rocks.|
73256|Wankanki Supersuite|73437|5|Briefly described|p151, p153|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Emplaced during Mount West Orogeny.|1345-1293 Ma||||Metagranite and gneiss.|
33646|Wankari Volcanics|24496|5|Briefly described|p15|Mesoproterozoic|Mesoproterozoic|Of Tjauwata Group. Geological Province: Musgrave Block.||||||
33646|Wankari Volcanics|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. Porphyritic rhyolite with rare epidotised and amygdaloidal mafic volcanics. Geological Province: Musgrave Block.||||||11-JAN-05
33646|Wankari Volcanics|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Rhyolite. Geological Province: Musgrave Block. Of Tjauwata Group.||||||14-JAN-05
33646|Wankari Volcanics|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. Porphyritic rhyolite with rare epidotised and locally amygdaloidal mafic volcanics. Age: ~1041Ma.||||||03-AUG-09
33646|Wankari Volcanics|61524|5|Briefly described|p17 Fig.1|Mesoproterozoic|Mesoproterozoic|Part of rift sequence along with Tjauewata Group and Bloods Range Beds. Geological Province: Musgrave Province.||||||
33646|Wankari Volcanics|61864|6|Mentioned|p18 fig 4|||Part of a rift sequence.||||||
33646|Wankari Volcanics|62989|5|Briefly described|p39|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. Age: 1041+/-2Ma. Pervasively overprinted by the Petermann Orogeny.||||||25-JAN-07
33646|Wankari Volcanics|64745|5|Briefly described|p376|Stenian|Stenian|Uppermost unit of Tjauwata Supercrustal. Age: ca. 1.04Ga. Correlated with Hogarth Formation (Tollu Group).||||||
33646|Wankari Volcanics|65135|6|Mentioned|p16|Stenian|Stenian|Dated at 1041 +/- 2 Ma.||||||
33646|Wankari Volcanics|65833|5|Briefly described|p16|Stenian|Stenian|Of Tjauwata Group. 1041 +/- 2 Ma: a c.30 m.y. time gap between this unit and the Puntitjata Rhyolite, also of the Tjauwata Group.||||||
33646|Wankari Volcanics|65906|5|Briefly described|p6, p19|Mesoproterozoic|Mesoproterozoic|A series of porphyritic felsic volcanics interlayered with minor mafic volcanic units. Correlative of the Hogarth Formation, Tollu Group. Age: 1041+/-2 Ma. Unit in the Tjauwata Group.||||||
33646|Wankari Volcanics|67128|5|Briefly described|p13, p30-31|||Bloods Range. Coeval with granite magmatism in the central Musgrave Province to the east.|1051 +/- 22 Ma (SHRIMP).|Tjauwata Group.|||Locally amygdaloidal, fine-grained, porphyritic felsic volcanics with minor interlayered mafic units. Includes porphyritic rhyolite with rare epidotized and amygdaloidal mafic volcanics.|
33646|Wankari Volcanics|69436|5|Briefly described|p21:13-14, 19|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Kober Pb-Pb zircon age.|1041 +/- 2 Ma (Scrimgeour et al., 1999).|Tjauwata Group.||Is overlain by Bloods Range Formation. Is correlated with Puntitjata Rhyolite.|A succession of fine-grained, porphyritic, felsic volcanic rocks with minor interlayered mafic units.|12-JUL-16
33646|Wankari Volcanics|69606|6|Mentioned|p5|||Musgrave Province.|1041+/-2 Ma|Tjauwata Group, upper part||||
33646|Wankari Volcanics|70018|5|Briefly described|p233,235|Mesoproterozoic|Mesoproterozoic|Amadeus Basin. SHRIMP U-Pb age of 1051+\-22 Ma; Scrimgeour et al., 1999).|1051+\-22 Ma|Unit of Tjauwata Group.||Overlain conformably by Bloods Range Formation. Underlain by Puntitjata Rhyolite.||
33646|Wankari Volcanics|71210|5|Briefly described|p9|Stenian|Stenian|Correlation with the Hogarth Formation was established by Close et al., 2003a.||Tjauwata Group||Equivalent to the Hogarth Formation.||
33646|Wankari Volcanics|71211|6|Mentioned|p234||||ca. 1040 Ma|||||
33646|Wankari Volcanics|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||basic volcanic rock, rhyolite|
33646|Wankari Volcanics|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Sample GSWA 210702 (schistose, porphyritic rhyolite) yielded a regression intersecting concordia curve at 1044+\-8 Ma, interpreted as magmatic crystallisation age of the rhyolite. Sample GSWA 208439 (metarhyolite) yielded a regression intersecting concordia curve at 1039+\-7 Ma, interpreted as magmatic crystallisation age of the metarhyolite. Sample GSWA 208498 (quartzite) yielded a weighted mean 207Pb/206Pb age of 1105+\-24 Ma, interpreted as maximum depositional age of sandstone protolith. See 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeol_lut.csv.|1051-1039 Ma (inferred)|Unit of Tjauwata Group.|||Quartzite; blocky to flaggy, muscovite-bearing; sericite schist, massive to quartz-amygdaloidal basalt, quartz-feldspar-phyric metarhyolite; quartz-feldspar-phyric schist and felsic intrusives.|
33646|Wankari Volcanics|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1051+/-22 Ma (crystallisation: U-Pb zircon SHRIMP)||||Volcanic rock.|
23136|Wanneroo Member|12759|2|Defined|p37; p28 Tb. 7; p32 Fig 15; P36 Fig 17|Aptian||Named from: Wanneroo townsite, N of Perth. Type Section: Bore AM 24, 223-423 m depth (max 450 m) at AMG Zone 50, 389624 m E, 6491151 m N.||Member of Leederville Formation.||Conformably overlain by Pinjar Member and underlain conformably by South Perth Shale or Mariginiup Member. See text for other relationships.|Discontinuous interbedded sandstones, siltstones and shales of marine and non-marine origin; individual sand beds generally 12-15 m thick; granitic scree boulders common in SE margin of Perth Region.|12-MAY-14
23136|Wanneroo Member|67115|5|Briefly described|p63, p64, p70 |Cretaceous|Cretaceous|Forms the main aquifer. Thickness varies from 108 to 265 m. Lithology and trace elements detailed.||Unit in Leederville Formation.||Conformable transitional contact with the underlying Mariginiup Member; is overlain by the Pinjar Member.|Interbedded silty sandstones and shales of marine and continental origin.|
23136|Wanneroo Member|68254|5|Briefly described|p1040 Tb.3, p1046 Tb. 4|||Member status specified in column heading of Table 3. Wanneroo Formation and Wanneroo Member used interchangeably in this paper.||Of the Leederville Formation||||
23136|Wanneroo Member|68811|6|Mentioned|p180 tbl 39|Cretaceous|Cretaceous|||Of Leederville Formation.||||15-APR-20
73257|Warakurna Supersuite|63864|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes Giles Suite.||||||
73257|Warakurna Supersuite|64408|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Date shown: 1050-1178 Ma, (S. S. Sun 1996), for Giles Complex. Subdivided into 3 unnamed and one informally named unit.||||||16-SEP-08
73257|Warakurna Supersuite|64580|6|Mentioned|map legend|||||||||
73257|Warakurna Supersuite|65135|5|Briefly described|p1, p6 Fig.4, p12 Fig.8, p13-14, p16||Stenian|Groups all igneous rocks related to the ~1075 Ma Giles Event. Minimum age of ~1078 Ma. Contains Skirmish Hill Volcanics. Crops out over ~1.5 million sq km of central and western Australia, forming the Warakurna Large Igneous Province. In the western Musgrave Complex, largely occurs within and to the SW of the Tjuni Purlka Tectonic Zone||||||
73257|Warakurna Supersuite|65506|5|Briefly described|p986, p987 Fig. 1A||c.1070 Ma.|Also known as Warakurna Large Igneous Province. Overlies the Collier Group. Sills form part of Bangemall Supergroup.||||||
73257|Warakurna Supersuite|65693|5|Briefly described|p1, p3, p5, pp8-15.|Mesoproterozoic|Mesoproterozoic|The magmatic expression of the Giles Event: mafic and felsic intrusions outcropping over 1.5 million km2 of central and western Australia; took place over c.60 m.y. Hosts Ni-Cu-PGE mineralization.|c.1078 - c.1067 Ma.||Includes Skirmish Hill Volcanics and Alcurra Suite, as well as un-named layered intrusions and massive gabbro.|||
73257|Warakurna Supersuite|65833|5|Briefly described|p1, p6-7 Figs.4-5, p12 Fig.8, p13-16|Stenian|Stenian|Groups all igneous rocks related to the ~1075 Ma Giles Event. Includes layered mafic-ultramafic intrusions, unlayered gabbro and comagmatic leucogranite, and possible remnants of bimodal volcanics. Magmatism may have occurred as punctuated events over 60 m.y. Crops out across ~1.5 million sq. km in central and western Australia. A-type character. Includes Skirmish Hill Volcanics.||||||
73257|Warakurna Supersuite|65898|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes Giles Suite mafics and ultramafics (>1078 Ma) and 9 ungrouped unnamed granitic units (1075-1060 Ma).||||||
73257|Warakurna Supersuite|65899|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age shown as c.1070 Ma. Includes Glenayle and Prenti Dolerites.||||||
73257|Warakurna Supersuite|65906|5|Briefly described|p3-4|||Gabbros, granites and mafic dykes. West Musgrave Block. Contains all igneous rocks related to the c.1080 Ma Giles Event: Bentley Supergroup and Giles Complex.||||||
73257|Warakurna Supersuite|65907|6|Mentioned|p6.|||Interpreted as a mantle plume event.||||||
73257|Warakurna Supersuite|66104|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Shown as consisting of Kulkatharra Dolerite sills which intrude into the Edmund and Collier Groups. Age shown as c.1070 Ma.||||||
73257|Warakurna Supersuite|66256|5|Briefly described|p4 Fig.3, p11 Fig.8, p16, see comments|Stenian|Stenian|In west Musgrave Province. Intruded mainly along tectonic margins of Tjuni Purlka Tectonic Zone. In Musgrave Province, incorporates Giles intrusions (giant layered mafic-ultramafic intrusions). Age: 1073, 1074 and 1075 Ma, SHRIMP, Whole rock Nd isotopic data, 6 analyses (GSWA and GA). Geochron (SHRIMP) results for crystallization age: Mamutjarra Zone 1026+/-26 to 1078+/-3 Ma; Tjuni Purlka Tectonic Zone 1052+/-11 to 1078+/-5 Ma. Sources: GSWA and GA. See also p18 Fig.14, p29 Fig.26, p31-32, p41, p53-54 App.1, 57-59 App.3, p71 App.4.|||||Includes locally rapakivi-textured, syenogranites, quartz syenites, and monzogranites.|11-JAN-17
73257|Warakurna Supersuite|66280|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age shown as >1078-1060 Ma. Includes Giles Suite and several unnamed units: mylonitic syenogranite and leucogranite; fine-grained leucocratic syenogranite; porphyritic to seriate syenogranite; and massive biotite syenogranite. ||||||
73257|Warakurna Supersuite|66281|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic||||Includes Giles Suite and un-named units of olivine gabbro, syenogranite and monzodiorite.||Mafic intrusive rocks and layered mafic-ultramafic intrusives.|
73257|Warakurna Supersuite|66282|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|In this map area, is shown as consisting of Giles Suite rocks aged >1078 Ma as well as four separately-mapped but un-named more felsic intrusive units aged 1075 - 1060 Ma..|>1078 - 1060 Ma.||Includes Giles Suite.||Intrusive mafic and ultramafic rocks, variably metamorphosed; minor felsic intrusives: syenogranite, granodiorite, monzogranite.|
73257|Warakurna Supersuite|66284|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Apart from Giles Suite, includes a syenogranite with mafic xenoliths.|||Includes Giles Suite and an un-named but separately-mapped syenogranite unit.|||
73257|Warakurna Supersuite|67128|4|Described|p5 Fig.3, p6-7, p10-11|||All magmatic rocks formed during the Giles Event in the western Musgrave Province. Voluminous mafic and A-type felsic intrusions. Thought to have formed during the Warakurna LIP magmatism.|>1078 to c.1026 Ma.||Giles intrusions, Alcurra Dolerite.|Intrudes the Tollu Group.|Layered mafic-ultramafic intrusions, massive gabbros, mafic dykes, and rare granitic rocks.|
73257|Warakurna Supersuite|67136|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|c.1070 Ma.||Includes Kulkatharra Dolerite.|Intrudes Edmund and Collier Groups.||
73257|Warakurna Supersuite|67244|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Also contains five separately-mapped but un-named sub-units.|1078 - 1074 Ma.||Includes Giles Suite and Alcurra Dolerite.|||
73257|Warakurna Supersuite|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Map includes 17 separate, un-named units. Ultramafic intrusives and granites.|1078 - 1060 Ma.||Includes Giles Suite, Alcurra Dolerite, and 17 un-named units.||Layered mafic-ultramafic intrusions; dolerite dykes, sills and plugs; granitic intrusions.|
73257|Warakurna Supersuite|67375|3|Fully described|p5, p13, pp33-38, pp216-230, pp340-347.|Mesoproterozoic|Mesoproterozoic|Groups all igneous intrusive and extrusive rocks related to the 1085-1040 Ma Giles Event. Outcropping across 1.5 million km2 of central and western Australia, it forms the Warakurna Large Igneous Province. Mafic to felsic magmatism; granites have a strong A-type geochemical signature. Hosts economically significant mineral deposits.|1078 +/- 3 - 1062 +/- 10 Ma.||Includes Bentley Supergroup, Giles Suite and Alcurra Dolerite.|Intrudes Wankanki Supersuite.|Giant layered mafic-ultramafic 'Giles intrusions', massive gabbros mixed amd mingled with granite, dolerite, granite plutons, and mafic and felsic lavas.|10-NOV-15
73257|Warakurna Supersuite|67553|4|Described|p2,7-8,11-12,15-17,20,27,31,34-35|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Mafic and felsic intrusions into rocks of the Musgrave Province during 1085-1040 Ma Giles Event. Outcrops across ~1.5 million km2 of central and western Australia, forming the Warakurna LIP (Wingate et al., 2004; Morris and Pirajno, 2005). Volcanic components of the Warakurna Supersuite are also grouped as part of the Bentley Supergroup. Associated with the Ngaanyatjarra Rift, a long-lived intracontinental rift setting. Locally strongly deformed during the Petermann Orogeny (coinciding with global Pan-African period of plate reorganisation during Gondwanan assembly). Deposition occuring at ?1085-?1040 Ma (GSWA data). See also p38,58,73,95.|c. 1085-1040||Includes Alcurra Dolerite, Giles intrusions and Kunmarnara Group.|||
73257|Warakurna Supersuite|68077|5|Briefly described|p3 Fig.1, p5-6, p11, p19-23, p31-38|Mesoproterozoic|Mesoproterozoic|Emplaced during the 1085-1040 Ma Giles Event; over at least 1.5 million km2 to form the Warakurna Large Igneous Province. Isotopic composition (Lu-Hf and Sm-Nd) and evolution tabulated and discussed in detail.|1075-1067  Ma (U-Pb zircon)||||Dolerite, basalt, komatiite, gabbro, granophyre, basaltic andesite, gabbronorite, troctolite, norite, olivine and biotite gabbros.|07-SEP-17
73257|Warakurna Supersuite|68100|5|Briefly described|p2, 5, 7, 15, 26, 28, 32, 33|Mesoproterozoic|Mesoproterozoic|Includes giant layered-mafic intrusions (Giles intrusions), mafic dykes, and granites.|1075-1060 Ma|||Intrudes/overlies Kunmarnara Group|Layered mafic intrusions, mafic dykes and granites. Locally rapakivi textured granites. Includes charnokitic syenogranite.|19-JAN-17
73257|Warakurna Supersuite|68186|5|Briefly described|p30|Mesoproterozoic|Mesoproterozoic|Wingate et al. (2004). Widespread unit.|c.1075 Ma.|||||
73257|Warakurna Supersuite|68561|6|Mentioned|500K_GEOLOGYP08_LUT.csv||Mesoproterozoic|||||||23-OCT-15
73257|Warakurna Supersuite|68995|5|Briefly described|p1-2, p5, p22, p28-33, p43, p46 Fig.22|Stenian|Stenian|Volcanic rocks are the dominant lithology of the Bentley Basin. Geochemistry briefly discussed. See also p48 Fig.24, p54 Fig.29, p57 Fig.31, p59, p66, p74.|c. 1080 - 1045 Ma (SHRIMP U-Pb)||||Massive gabbro, bimodal magmatic and volcanic rocks including leucogranite, monzogranite, alkali-feldspar granite and alkali-feldspar syenite.|
73257|Warakurna Supersuite|68996|5|Briefly described|p5, 25, 28-29, 32, 35-47, 53, 54, 65,66|Mesoproterozoic|Mesoproterozoic|Age is of granite component. See also Warakurna granite p59.|1065 +/- 9 Ma||Includes Tollu granite, Winburn granite||Granites, quartz syenite, massive fine grained granodiorite, mylonitic syenogranite. Density ranges from 2.56->2.9g/cm^3.|
73257|Warakurna Supersuite|69003|5|Briefly described|p4, p37, p39, p49, p51-52, p59|Mesoproterozoic|Mesoproterozoic|W Musgrave Province, Paterson Orogen. Associated with Giles Orogeny. Includes the mainly felsic extrusive rocks of the Bentley Supergroup. Some units quarried for high-quality dimension stone.|||Giles intrusions.||Granite, gabbro, layered mafic-ultramafic intrusions.|
73257|Warakurna Supersuite|69009|5|Briefly described|Map Legend||||||Includes Alcurra Dolerite and Giles Suite.||Comprises layered mafic-ultramafic intrusions; magnetite; dolerite sills/dykes/plugs; granitic and rhyolitic rocks.|
73257|Warakurna Supersuite|69010|6|Mentioned|Map Legend|||Warakurna Large Igneous Province.|||Includes the Kulkatharra Dolerite.|||
73257|Warakurna Supersuite|69091|4|Described|p52 Fig.4.1, p53, see comments|Mesoproterozoic|Mesoproterozoic|Intrudes rocks of Musgrave Region (in geographical sense denotes general area in which Mesoproterozoic rocks of Musgrave Province outcrop). Formed during c. 1085 Ma to c. 1040 Ma Giles Event. Craton scale mafic magmatism (c. 1078-1073 Ma), basis for grouping igneous rocks into Warakurna Large Igneous Province (Wingate et al., 2004; Morris and Pirajno, 2005). Volcanic components of Warakurna Supersuite are grouped into Bentley Supergroup. See also Warakurna granite (p137 Fig.6.4 and p138 Fig.6.5). See also p54 Fig.4.2, p55 Fig.4.3, p58, p59 Fig.4.6, p69, p73 Fig.4.16, p82, p86, p131 Fig.6.1, p134 Fig.6.2, p141 Fig.6.8, p183, p205-206.|1085-1040 Ma||Kunmarnara Group, Bentley Supergroup, Giles Suite, Winburn Granite.||A-type granites; leucogranite, gabbro, layered mafic-ultramafic intrusions.|
73257|Warakurna Supersuite|69152|5|Briefly described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic||||Includes Giles Suite|||
73257|Warakurna Supersuite|69153|5|Briefly described|GEOL_LUT_CSV files; GEOCHRON files|Mesoproterozoic|Mesoproterozoic|Tollu pluton' (185583) was dated (SHRIMP-B) at 1073+/-6 Ma, and is interpreted as the age of igneous crystallization of the granite. See GEOCHRON/194759.1.pdf, 194637.1.pdf and 185583.1.pdf.|||Alcurra Dolerite|is cross-cut by Kullal Dyke Suite; intrudes Wankanki Supersuite|Dolerite sill/plug, granite, syenogranite, leucogranite, (alkali feldspar/qtz) syenite, (cpx) granodiorite, hbl-bio-qtz monzodiorite to granodiorite, hbl-bio monzogranite and syenogranite, tonalite.|12-NOV-15
73257|Warakurna Supersuite|69166|6|Mentioned|geologyp_lut.csv|Neoproterozoic|Neoproterozoic||||Includes Kulkatharra Dolerite|||
73257|Warakurna Supersuite|69167|4|Described|geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Age derived from dolerite sill sample (178187.1.pdf)|1050 +/- 22 Ma (SHRIMP)|||Intrudes Eel Creek Formation|Dolerite sill or plug; fine- to medium-grained dolerite and gabbro|
73257|Warakurna Supersuite|69185|5|Briefly described|500k_geologyp08_lut.csv|||Geological Province: Pilbara Craton.|||Includes Kilkatharra Dolerite.|||
73257|Warakurna Supersuite|69436|5|Briefly described|p21:1, 4, 10-12, 16|||Musgrave Province. Includes (Howard et al., 2011) all magmatic units formed during a second major phase of magmatism, during the Giles Event (1085-1040 Ma). Forms the Warakurna Large Igneous Province. Reworked by the Petermann Orogeny.|||Giles Complex, Alcurra Dolerite, Angatja Suite, Hull Suite, Michell Nob Granite, Nulchara Charnockite.||Mafic and ultramafic intrusive rocks.|12-JUL-16
73257|Warakurna Supersuite|69546|6|Mentioned|p115|Stenian|Stenian|Geological province: Musgrave Province. Associated with Giles Event.|1085-1040 Ma|||||
73257|Warakurna Supersuite|69554|6|Mentioned|p139|||Western Musgrave Province.|||||Orthogneisses.|
73257|Warakurna Supersuite|69583|5|Briefly described|p58, p82, p85, p92, p127; Plates 2, 3|Proterozoic|Proterozoic|Warakurna Large Igneous Province, northwestern and central Yilgarn Craton. Appears also on p58, p82 mis-spelt as Warrakuna Supersuite. Appears in seismic images as highly-reflective, shallow-dipping sills, hundreds of kilometres in extent and up to 200m thick.|c.1070 Ma.||Mount Holmes Gabbro.||Dolerite dykes, plugs and sills. Fine- to medium-grained dolerite and gabbro.|
73257|Warakurna Supersuite|69590|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Of Warakurna Large Igneous Province. Events: Warakurna Supersuite Magmatic Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv.|1084-1047 Ma (inferred)||||Dolerite sill or plug; fine- to medium-grained dolerite and gabbro|
73257|Warakurna Supersuite|69596|6|Mentioned|p13||||||Kulkatharra Dolerite.|||
73257|Warakurna Supersuite|69655|5|Briefly described|p1-p2, p4-p5-p7, p57|Stenian|Stenian|Musgrave Province. Emplaced during the Giles event (which is the source of the age). Outcrops across approximately 1.5 million square kilometers in central and western Australia forming the Warakurna Large Igneous Province.|||Includes the Alcurra Dolerite.||Granites, gabbro and layered mafic-ultramic intrusions.|
73257|Warakurna Supersuite|69729|5|Briefly described|p68-69, p74 Fig.8, p75, p78-79, p81-82|||See also p66 Fig.1. Musgrave Province. This unit groups all the magmatic products of the c.1090-c.1040 Ma Giles Event. Bimodal volcanic rocks of this unit also form the main component of the Bentley Supergroup. Geochemistry detailed.|||||Granites, gabbro, layered mafic-ultramafic Giles intrusions.|
73257|Warakurna Supersuite|70083|6|Mentioned|p206-207|||Western Musgrave Inlier. Associated with the Giles Event.|1085-1040 Ma.||||Granites.|
73257|Warakurna Supersuite|70084|5|Briefly described|p220|Stenian|Stenian|Geological province: Musgrave Province, Paterson Orogen.|||Includes Bentley Supergroup.|||
73257|Warakurna Supersuite|70095|5|Briefly described|p17|||Geological province: Musgrave Province. Of Bentley Basin.|||Includes Bentley Supergroup, Winburn granite, Giles intrusions and Kunmarnara Group.|Overlain by Buldya Group.||
73257|Warakurna Supersuite|70132|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|1084-1067 Ma.||Kulkatharra Dolerite.|||
73257|Warakurna Supersuite|70134|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin. The five facies are mapped separately.|1078-1060 Ma.||Giles Suite.||Granitic rock, undivided; K-feldspar-phyric (to 5cm) quartz syenite, locally rapakivi textured; foliated hornblende-bearing syenogranite with mafic enclaves; leucocratic porphyritic to seriate syenogranite; coarse-grained tourmaline vein, foliated.|
73257|Warakurna Supersuite|70136|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|||Kulkatharra Dolerite.|||
73257|Warakurna Supersuite|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||1078-1062 Ma.|||Intrudes Frank Scott Formation (Mission Group), Scamp and Mount Waugh Formations.|Granitic rock, undivided; fine- to medium-grained quartz syenite containing K-feldspar phenocrysts up to 5cm, locally with rapakivi texture; dolerite sill or plug of fine- to medium-grained dolerite, and gabbro.|
73257|Warakurna Supersuite|70140|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|c.1070 Ma.||||Dolerite sill or plug; fine- to medium-grained dolerite and gabbro.|
73257|Warakurna Supersuite|70153|5|Briefly described|100k_geologyp10_lut.csv|Mesoproterozoic|Mesoproterozoic||||Includes Giles Suite.|||
73257|Warakurna Supersuite|70226|5|Briefly described|map legends|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|1084-1047 Ma||||Dolerite sill or plug; fine- to medium-grained dolerite, and gabbro.|16-DEC-15
73257|Warakurna Supersuite|70419|5|Briefly described|p15-17, p23|Proterozoic|Proterozoic|Sills of this unit produce a highly reflective and gently N-dipping unit in seismic line 10GA-YU2. Appears as Warakurna Suite on p17.||||Correlates with Mount Holmes Gabbro.||
73257|Warakurna Supersuite|70619|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Warkurna Large Igneous Province.|||Includes Giles Suite.||Granite; metagranite; amphibolite; gabbro; metagabbro.|03-JUN-16
73257|Warakurna Supersuite|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|Samples of granite (195231.1.pdf) are the sources for SHRIMP dates.|1055 Ma  (Isotopic)  1079 Ma +/- 8 Ma (SHRIMP)|Musgrave Complex|Includes Alcurra Dolerite, Giles Suite 1, Giles Suite 2, Giles Suite 1 (2), Bentley Supergroup|Intrudes into Wankanki Supersuite, Pitjantjatjara Supersuite|Granitic rock, quartz syenite, alkali feldspar granite, alkali feldspar quartz syenite, granodiorite, monzodiorite, monzogranite, pegmatitic leucogranite, mylonitic leucogranite, mylonitic syenogranite, syenogranite, tonalite, dolerite and gabbro.|
73257|Warakurna Supersuite|70763|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|||Giles Suite.|||
73257|Warakurna Supersuite|70767|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|||Kulkatharra Dolerite.|||
73257|Warakurna Supersuite|70768|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|||Kulkatharra Dolerite.|||
73257|Warakurna Supersuite|70770|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Warakurna Large Igneous Province.|||||Dolerite sill or plug; fine- to medium-grained dolerite and gabbro.|
73257|Warakurna Supersuite|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province. Of Warakurna Large Igneous Province. Includes all igneous and intrusive rocks of the 1093-1045 Ma Giles Event (Smithies et al., 2009). Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Warakurna Supersuite Magmatic Event (1084-1040 Ma); Giles Event (1085-1040 Ma). Sample GSWA 174589 (quartz syenite dyke) yielded an interpreted (weighted mean 207Pb*/206Pb*) crystallisation age of 1074+\-3 Ma for the syenite dyke. Sample GSWA 174662 (granophyre) yielded an interpreted (207Pb/206Pb concordia) magmatic crystallisation age of 1077+\-6 Ma. Sample GSWA 183474 (hornblende syenogranite) yielded an interpreted (207Pb/206Pb concordia) magmatic crystallisation age of 1072+\-8 Ma. Sample GSWA 183847 (syenite; also part of Kunmarnara Group) yielded an interpreted (regression intersecting concordia curve) magmatic crystallisation age of 1078+\-4 Ma. Sample GSWA 185509 (leucogranite) yielded an interpreted (weighted mean 207Pb*/206Pb*) magmatic crystallisation age of 1075+\-3 Ma. Sample GSWA 185583 (pophyritic granite) yielded an interpreted (regression itersecting concordia curve) igneous crystallisation date of 1073+\-6 Ma. Sample GSWA 187054 (quartz diorite) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) magmatic crystallisation age of 1055+\-10 Ma. Sample GSWA 187256 (granite dyke) yielded an interpreted (weighted mean 207Pb*/206Pb*) magmatic crystallisation age of 1066+\-9 Ma. Sample GSWA 189563 (hbl-bt syenogranite) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) igneous crystallisation age of 1065+\-9 Ma. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv + other geochron files for additional geochronological analyses.|1084-1047 Ma (inferred)||Includes Alcurra Dolerite, Giles Suite.|Intrudes ino Wankanki and Pitjantjatjara supersuites.|Pegmatitic leucogranite, dolerite sill or pug, leucocratic tonalite, quartz syenite, syenogranite, monzogranite, rhyolite, granodiorite, granite.|
73257|Warakurna Supersuite|70794|5|Briefly described|2_5m_interpdykel15_lut.csv|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province|1084-1047 Ma inferred||||Dolerite sill or plug, fine to medium grained dolerite and gabbro.|
73257|Warakurna Supersuite|70795|4|Described|2_5m_interpdykel15_lut.csv|Mesoproterozoic|Mesoproterozoic|Also 2_5m_interpgeop15_lut.csv|1084-1047 Ma||Includes Kulkatharra Dolerite||Dolerite sill or plugs, fine-medium grained dolerite, gabbro. Layered mafic-ultramafic intrusions, massive gabbro, granite and associated mafic to felsic volcanic rocks.|
73257|Warakurna Supersuite|70796|4|Described|2_5m_interpgeop15_lut.csv|Mesoproterozoic|Mesoproterozoic|Of the Warakurna Large Igneous Province. Affected by the following events: Alice Springs Orogeny (450  295 Ma); Petermann Orogeny (580  520 Ma); Paterson Orogeny (635  540 Ma); Warakurna Supersuite Magmatic Event (1084  1040 Ma); Giles Event (1090  1040 Ma). An inferred minimum age of 1040 Ma is also provided. See also 2_5m_interpdykel15_lut.csv, 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop14_lut.csv, Bungar100_2539_stratig.pdf, Yalgoo100_2241_stratig.pdf, Youanmi100_2640_stratig.pdf.|1084 +/ 9 Ma (Max age, isotopic)||||Layered maficultramafic intrusions, massive gabbro, granite, and associated mafic to felsic volcanic rocks. Diorite, minor syenogranite, dolerite sill or plug.|
73257|Warakurna Supersuite|70814|6|Mentioned|p37||||||||Mafic magmas.|
73257|Warakurna Supersuite|70826|6|Mentioned|p10, p14 tbl 5|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen, Musgrave Province, Yilgarn Craton.|1084-1047 Ma||Giles Suite, Alcurra Dolerite, Kulkatharra Dolerite, Prenti Dolerite||Mafic and locally felsic igneous rocks.|
73257|Warakurna Supersuite|70830|5|Briefly described|p22, p40|Stenian|Stenian|Youanmi Terrane. Misspelt as the Warakurna Suite on p40.|c. 1070 Ma|||||
73257|Warakurna Supersuite|70831|5|Briefly described|p2, p5-p6, p9|Stenian|Stenian|Musgrave Province.|c. 1085-1040 Ma||Includes the Alcurra Dolerite.||Layered mafic and ultramafic intrusions, mixed and mingled gabbros and leucogranites and bimodal volcanics.|
73257|Warakurna Supersuite|70839|5|Briefly described|p326-327,336,339,341-342,345|Stenian|Stenian|Geological province: Musgrave Province. Voluminous mafic and felsic mantle-derived intrusive and extrusive magmatic rocks associated with c. 1.09-1.04 Ga Giles Event (Smithies et al., 2015). Emplaced within Ngaanyatjarra Rift (Evins et al., 2010; Aitken et al., 2012).|c. 1.09-1.04 Ga||Includes Kunmarnara Group.|Underlain by, and interbedded with Kunmarnara Group and Bentley Supergroup.|Mafic and felsic intrusives and extrusives; sediments.|
73257|Warakurna Supersuite|71088|5|Briefly described|p4-p5, p25|||Musgrave Region. Mantle-derived.|1090-1040 Ma|||Overlies and interbeds with the Kunmarnara Group and Bentley Supergroup.|Mafic and felsic, intrusive and extrusive igneous rocks.|
73257|Warakurna Supersuite|71158|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.|1084-1067 Ma.|||||
73257|Warakurna Supersuite|71159|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Warakurna Large Igneous Province. The two facies are mapped separately.|||||Diorite to minor syenogranite in dykes and sills; dolerite sill or plug: fine- to medium-grained dolerite, and gabbro.|
73257|Warakurna Supersuite|71169|5|Briefly described|p81-p82|Stenian|Stenian|Musgrave Province. |1085-1040 Ma||||Dolerite sills.|
73257|Warakurna Supersuite|71170|5|Briefly described|p5-p6|||Emplaced during the Giles Event.|||||Gabbro, granites and layered mafic-ultramafic intrusions.|
73257|Warakurna Supersuite|71210|6|Mentioned|xv, p8, p20, p97, p99, p112, p131, p134|||Musgrave Province.|c. 1090 - 1040 Ma||Includes the Giles Suite.|||
73257|Warakurna Supersuite|71211|6|Mentioned|p6, p7 fig 1.4, p10, p24 fig 2.1|||See also  p84 fig 3.1, p85, p136 fig 4.1, p216, p231.|||||Granites, gabbros and layered mafic-ultramafic intrusions.|
73257|Warakurna Supersuite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Of Warakurna Large Igneous Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Warakurna Supersuite Magmatic Event (1084-1040 Ma); Giles Event (1085-1040 Ma). Sample GSWA 174662 (granophyre) yielded a concordia age of 1077+\-6 Ma, interpreted as the magmatic crystallization age of the granophyre. Sample GSWA 174761 (porphyritic granite dyke) yielded a weighted mean 207Pb/206Pb date of 1075+\-7 Ma, interpreted as the magmatic crystallization age of the granite dyke. Sample GSWA 183474 (hbl syenogranite) yielded a concordia intercept date of 1072+\-8 Ma, interpreted to be magmatic crystallisation age. Sample GSWA 185486 (porphyritic microgranite) yielded a concordia age of 1072+\-5 Ma, interpreted as magmatic crystallisation age of the microgranite. Sample GSWA 185509 (leucogranite) yielded a weight mean 207Pb/206Pb age of 1075+\-3 Ma, interpreted to be magmatic crystallisation age. Sample GSWA 185583 (k-spar granite) yielded a regression intersecting concordia curve at 1073+\-6 Ma ,interpreted as igneous crystallisation age. Sample GSWA 208453 (syenogranite) yielded a regression intersecting concordia curve at 1063+\-8 Ma, interpreted as magmatic crystallisation age of the syenogranite. Sample GSWA 208486 (migmatitic metasyenogranite) yielded a weighted mean 207Pb/206Pb age of 1031+\-6 Ma, interpreted as magmatic crystallisation age. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv.|1084-1047 Ma (inferred)||Includes Alcurra Dolerite, Giles Suite.||Pegmatitic leucogranite, dolerite sills and gabbro, tonalite, syenite, syengogranite, monzogranite, granite, leucogranite; metamorphosed.|
73257|Warakurna Supersuite|71269|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Of Warakurna Large igneous Province. Events: Alice Springs Orogeny (450 - 295 Ma); Petermann Orogeny (580 - 520 Ma); Paterson Orogeny (635 - 540 Ma); Warakurna Supersuite Magmatic Event (1084 - 1040 Ma); Giles Event (1085 - 1040 Ma). See 500k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv, 2_5m_interpdykel15_lut.csv.|1084-1040 Ma (inferred)||||Diorite to minor syenogranite in dykes and sills; dolerite sill or plug; fine- to medium-grained dolerite, and gabbro.|
73257|Warakurna Supersuite|71270|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Kepa Kurl Booya Province, Albany-Fraser Orogen, West Australian Craton. Events: Albany-Fraser Orogeny Stage II (1225 - 1140 Ma); Albany-Fraser Orogeny (1330 - 1140 Ma); Albany-Fraser Orogeny Stage I (1330 - 1260 Ma); Biranup Orogeny (1710 - 1650 Ma); Ngadju Event (1780 - 1760 Ma); Salmon Gums Event (1815 - 1800 Ma); Tropicana Event (2520 - 2505 Ma); Atlantis Event (2720 - 2550 Ma). See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 100k_geologyp14_lut.csv, 500k_interpgeop_lut.csv, 2_5m_interpgeop15_lut.csv, 2_5m_interpdykel15_lut.csv.|1084+\-9 Ma; 1040 Ma||Includes Giles Suite, Prenti Dolerite.||Layered mafic-ultramafic intrusions, massive gabbro, granite, and associated mafic to felsic volcanic rocks.|
73257|Warakurna Supersuite|71321|6|Mentioned|p5|Stenian|Stenian|Geological province: Musgrave Province.|1085-1040 Ma|||||
73257|Warakurna Supersuite|71416|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province.||||||
73257|Warakurna Supersuite|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1074+/-3 Ma (crystallisation: U-Pb zircon).||||Microgranite, rhyolite, quartz syenite dyke.|
73257|Warakurna Supersuite|71891|6|Mentioned|p8|||||||||
73257|Warakurna Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic||max age 1084+/-6 Ma, min age ~1040 Ma inferred.||Includes Giles Suite 1, Giles Suite 2.||Layered mafic-ultramafic intrusions, massive gabbro, granite, + associated mafic to felsic volcanic rocks; Dolerite sill/plug; fine- to medium-grained dolerite, and gabbro; Strongly foliated biotite metamonzogranite; medium-grained; equigranular;|
73257|Warakurna Supersuite|72094|4|Described|p2, p3, 4, 12, 13, 14, p15-16, 17, 18|Stenian|Stenian|Musgrave Province.  Suite of igneous rocks associated with Giles event. Intrudes Mount Palgrave and Pussy Cat Groups, and U-Pb magmatic crystallization zircon ages of 1071+/-5, 1063+/-8 and 1049+/-8 Ma suggest that Warakurna Supersuite intruded and formed source of volcano-sedimentary succession in Talbot Sub-basin. Summary table of zircon geochronology on p8 Table 1.  Reference made to Warakurna Large Igneous Province on p17. Associated with Giles Event Stage 3 3.|c. 1071+/-5 - 1031+/-6 Ma||Includes Giles intrusions, G2 gabbros, Alcurra Dolerite intrusions and bimodal volcanic rocks of the Talbot Supervolcano.|Unconformably overlain by Cobb Embayment sediments. Intrudes Talbot Sub-basin rocks.|Quartz, synenite and syenogranitic rocks. Dolerite, gabbro, layered mafic-ultramafic intrusions.|
73257|Warakurna Supersuite|72242|5|Briefly described|p29-30,32|Stenian|Stenian|Geological province: Coompana Province, Western Gawler Craton. Includes a massive olivine dolerite and microgabbro drilled in CDP002, dated at 1074+\-6 Ma (magmatic crystallisation age; Jagodzinski and Bodorkos 2018).|1078-1070 Ma||Includes Mallabie Volcanics and Gaints Head Suite.|||
73257|Warakurna Supersuite|72344|5|Briefly described|p3, p7-p9, p35, p44|||Coompana Province. Petrography, SHRIMP analyses and geochemistry are discussed for several samples. See also p143.|||Includes the Mallabie Volcanics and Giants Head Suite.|||
73257|Warakurna Supersuite|72443|5|Briefly described|p737-738||||||Includes the Alcurra Dolerite and the Winburn Granite.|||
73257|Warakurna Supersuite|72934|6|Mentioned|p4, p11-12, App.A|||Yielded a U-Pb SIMS zircon magmatic crystallisation age of 1074 +/- 6 Ma. Part of the Warakurna large igneous province/Ngaanyatjarra Rift[?].||||||
73257|Warakurna Supersuite|72947|6|Mentioned|p8-9, p17, p19-20|Stenian|Stenian|Of the Warakurna Large Igneous Province. Suggested to be contemporaneous with the Giants Head and Warbla Suites, extending the LIP over 400 km south, into the Coompana Province .|c. 1085 - 1030 Ma||Warbla Basalt[?], Warbla Suite, Giants Head Suite.|||
73257|Warakurna Supersuite|73058|5|Briefly described|p761 Fig.1, p768-769, p771-772, p774-776|Stenian|Stenian|Musgrave Province. Formed the Warakurna Large Igneous Province during the c.1075 Ma Giles Event, c. 10km thick sequence of bimodal volcanic rocks. Felsic rocks are strongly ferroan and alkalic-calcic, extreme enrichments in REE and HFSE. Nd model ages suggest mantle extraction event at 1700 Ma. Inferred additional significant juvenile mantle additions are masked in Hf isotope record by HFSE enriched crustal sources. Location in text includes p773 Tb.5, p777 Fig.14.|c. 1085-1040 Ma||Giles intrusions||Includes mafic-felsic volcanic rocks, layered mafic-ultramafic intrusions, granites, gabbros, and minor sedimentary rocks, local ultramafic cumulates.|
73257|Warakurna Supersuite|73091|6|Mentioned|Mapsheet||||||Includes the Giants Head Suite.|||
73257|Warakurna Supersuite|73177|5|Briefly described|p1100, 1114 Fig.16|||Musgrave Province.|1085-1050 Ma.|||||
73257|Warakurna Supersuite|73224|6|Mentioned|p42|Stenian|Stenian||c. 1074 Ma||Giants Head Suite, Mallabie Basalt, Warbla Suite|||
73257|Warakurna Supersuite|73225|5|Briefly described|p4||||c.1074 Ma.||Giants Head Suite, Warbla Suite, Mallabie Basalt.|||
73257|Warakurna Supersuite|73234|6|Mentioned|p19|Stenian|Stenian|Musgrave Province.|c. 1090-1040 Ma||||Includes igneous rocks.|
73257|Warakurna Supersuite|73346|6|Mentioned|p1-2, p4-6, p25|Mesoproterozoic|Mesoproterozoic|Produced during the 1085-1030 Ma Giles Event.|||||Includes mafic and felsic intrusive and extrusive magmatic rocks.|
73257|Warakurna Supersuite|73410|5|Briefly described|p7, 12|||Murchison Domain, Yilgarn Craton.|c.1075 Ma.||||East-striking, 50-150 km-long mafic, including dolerite, dykes.|
73257|Warakurna Supersuite|73437|5|Briefly described|p151, p153|Mesoproterozoic|Mesoproterozoic|Contains igneous rocks formed during the Giles Event.|||Giles Suite, West Hinckley Suite, Alcurra Dolerite||Igneous rocks including layered mafic-ultramafic intrusions, mixed and mingled gabbros and leucogranites, granite and dolerite intrusions, bimodal volcanic rocks.|
73257|Warakurna Supersuite|73641|6|Mentioned|p4||||||Warbla, Giants Head Suites; Mallabie Basalt.|||
73257|Warakurna Supersuite|74367|6|Mentioned|p23|||Musgrave Province.||||||
29116|Warambie Basalt|23244|5|Briefly described|p19|||||||||
29116|Warambie Basalt|23348|5|Briefly described|220|||||||||
29116|Warambie Basalt|23484|4|Described|p10 table 3|Archean|Archean|Of Whim Creek Group.  Maximum thickness:  500m.  Geological Province: Mallina Basin.||||||07-NOV-08
29116|Warambie Basalt|23784|5|Briefly described|p20|Archean|Archean|Of Whim Creek Group.||||||07-NOV-08
29116|Warambie Basalt|23789|5|Briefly described|p18 Tb. 4|Archean|Archean|Of the Whim Creek Group.  Max. thickness: 200m.  Geological Province: Pilbara Craton.||||||07-NOV-08
29116|Warambie Basalt|23793|4|Described|p22|Archean|Archean|Of Whim Creek Group.||||||07-NOV-08
29116|Warambie Basalt|23794|5|Briefly described|Map Legend|Archean|Archean|Of Whim Creek Group. Geological Province: Pilbara Craton.||||||07-NOV-08
29116|Warambie Basalt|24023|4|Described|p18|Archean|Archean|Of Whim Creek Group. Maximum thickness: 1000m.||||||07-NOV-08
29116|Warambie Basalt|24024|5|Briefly described|Map Legend|Archean|Archean|Of the Whim Creek Group. Geological Province: Pilbara Craton||||||07-NOV-08
29116|Warambie Basalt|24140|5|Briefly described|p214 Fig. 1, p217 Fig. 2|Archean|Archean|Of the Whim Creek Group. Basaltic lava, hyaloclastic and autobreccia; basaltic and granitic breccia.  Age of overlying Red Hill volcanics: c.3009+/-4Ma (Nelson 1998).  See also p216.Overlain by Red Hill Volcanics. Max. thickness: ~200m.||||||15-OCT-15
29116|Warambie Basalt|24184|4|Described|p713, 717|Archean|Archean|Of the Whim Creek Group. Geological Province: Mallina Basin. Age: ca.3010Ma (Hickman 2002).||||||07-NOV-08
29116|Warambie Basalt|24191|4|Described|p828, p831|Archean|Archean|Of Whim Creek Group.  Predominantly subaqeous, consisting of pillow breccia and abundant hylaoclastite - andesite, andesite basalt and subalkaline basalt. Underlies Red Hill Volcanics.  Geological Province: Pilbara Craton.||||||07-NOV-08
29116|Warambie Basalt|24541|5|Briefly described|p44|Archean|Archean|Of the Whim Creek Group. Age: c. 3010 Ma.||||||07-NOV-08
29116|Warambie Basalt|24550|5|Briefly described|p36 Tb. 3.2|Archean|Archean|Basal unit of the Whim Creek Group. Basalt (locally pillowed), minor sediments - dominantly subaqueous. Overlain by Red Hill Volcanics. Thickness: 200m. Geological Province: Pilbara Craton. See also p188 Tb. 8.2.||||||07-FEB-11
29116|Warambie Basalt|30766|2|Defined|Appendix|Precambrian|Precambrian|||||||
29116|Warambie Basalt|31310|6|Mentioned|Table 10|||Fitton and others 1975||||||
29116|Warambie Basalt|32954|6|Mentioned|p187|||||||||
29116|Warambie Basalt|34829|4|Described|p68|||Mentioned p67.||||||22-AUG-07
29116|Warambie Basalt|36551|6|Mentioned|p65|||||||||
29116|Warambie Basalt|38498|5|Briefly described|Table 1|||||||||
29116|Warambie Basalt|38544|6|Mentioned|Fig.1|||||||||
29116|Warambie Basalt|39697|4|Described|p108|||||||||
29116|Warambie Basalt|39837|6|Mentioned|Table 1|||||||||
29116|Warambie Basalt|41073|4|Described|p204|||||||||
29116|Warambie Basalt|41250|5|Briefly described|p29|||||||||
29116|Warambie Basalt|43595|5|Briefly described|p213|||||||||
29116|Warambie Basalt|43769|6|Mentioned|Fig.6,p861|||||||||
29116|Warambie Basalt|43821|5|Briefly described|map legend|Archean|Archean|Of Whim Creek Group.||||||07-NOV-08
29116|Warambie Basalt|44150|5|Briefly described|p129 Tb.2-15, p132 Fig.2-131, p137|||||Whim Creek Group|||Vesicular basalt to andesite, locally plagioclase-phyric; minor tuffaceous units near the base.|
29116|Warambie Basalt|50430|5|Briefly described|p167||Archean|3010 Ma. Parent: Whim Creek Group.||||||07-NOV-08
29116|Warambie Basalt|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Age: ~3.0Ga. Geological Province: Pilbara Craton.||||||07-NOV-08
29116|Warambie Basalt|63441|5|Briefly described|p5 Tb.1, p27|Archean|Archean|Of Whim Creek Group (Pilbara Supergroup). Underlies and partly interbedded with Red Hill Volcanics. Age: 3009+/-4Ma. Geological province: Whim Creek Basin, Pilbara Craton. Tholeiitic basalt lava, high-level intrusive sills, autobreccia and hyaloclastite.||||||07-FEB-11
29116|Warambie Basalt|63538|5|Briefly described|p31, p32, p6 Fig. 3|Archean|Archean|Of Whim Creek Group. Overlain by Red Hill Volcanics. Geological Province: Pilbara Craton. Typically tholeiitic.||||||19-APR-13
29116|Warambie Basalt|64174|5|Briefly described|Map legend|Archean|Archean|Of Whim Creek Group (De Grey Supergroup). Geol.prov: Whim Creek Basin, Pilbara Craton. Vesicular basalt and basaltic andesite, locally porphyritic, volcaniclastic and siliciclastic sedimentary rocks; metamorphosed.||||||01-JUL-14
29116|Warambie Basalt|64580|4|Described|map legend||Mesoarchean|Of Whim Creek Group. Vesicular basalt and basaltic andesite, locally porphyritic, volcaniclastic and siliciclastic sedimentary rocks; metamorphosed.||||||15-DEC-08
29116|Warambie Basalt|65415|5|Briefly described|p119 Fig.1, p120, p121.|Archean|Archean|Locally forms the base of Whim Creek Group. Is partly synchronous with the lower portion of Mount Brown Rhyolite Member.||Unit in Mons Cupri Volcanics.||Unconformably overlies Caines Well Granite. Locally interfingers with Mons Cupri Volcanics.|Tholeiites.|
29116|Warambie Basalt|66217|5|Briefly described|p39.|||Whim Creek Basin.||Unit in Whim Creek Group.||||
29116|Warambie Basalt|67201|4|Described|p7, p12, p16-17, p21, p27, p64-66|Archean|Archean|In northwestern Pilbara Craton, West Pilbara Superterrane, De Grey Superbasin, Whim Creek Basin.||Whim Creek Group||Unconformably overlies Whundo Group and folded Cleaverville Formation. Caines Well Granitoid Complex is source of granite boulders for coarse basal breccia of lower Warambie Basalt.|Coarse basal breccia. Vesicular basalt and basaltic andesite, locally porphyritic, volcaniclastic and siliciclastic sedimentary rocks; metamorphosed. Thick (~24 m) tabular flows and thin (0.5-2 m) irregular flows. Tholeiites enriched in Nb and Na2O.|25-NOV-16
29116|Warambie Basalt|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological province: Pilbara Craton. Of Central Pilbara Tectonic Zone; Of Mallina Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.||Unit of Whim Creek Group.|||Vesicular basalt and basaltic andesite, locally porphyritic, volcaniclastic and siliciclastic sedimentary rocks; metamorphosed|
29116|Warambie Basalt|69299|5|Briefly described|p6 Tb.1|Archean|Archean|Thickness on COOYA POOYA: 0-500 m.||Of Whim Creek Group.|||Vesicular and amygdaloidal basalt, pyroclastic units, hyaloclastite, and local pillow basalt; basal polymictic conglomerate and sandstone.|
29116|Warambie Basalt|69300|5|Briefly described|map legend|Archean|Archean|Whim Creek Basin (and Mallina Basin?), Whim Creek greenstone belt||Whim Creek Group||||
29116|Warambie Basalt|69301|5|Briefly described|p5 Fig.3, p9 Tb.1, p15|||Pilbara Craton. West Pilbara Superterrane. Whim Creek Basin.||Whim Creek Group|||Mafic volcanic rocks. Geochemistry - enrichment in Th and LREE.|
29116|Warambie Basalt|70022|6|Mentioned|p115|||West Pilbara Superterrane.||Whim Creek Group.||||
29116|Warambie Basalt|70775|4|Described|p12, p15, p24 tbl 3|Mesoarchean|Mesoarchean|Whim Creek Basin. The type area is located around the Warambie Homestead (Fitton et al., 1975) and here is 200m thick and is composed of vesicular, amygdaloidal and pillow basalt and basaltic andesite with rare intercalations of cherrrt and thin felsic volcaniclastic rocks. Between Mount Ada and Mount Oscar the stratigraphy of this unit is at least 500m thick and consists of basaltic breccia, hyaloclastite and vesicular and pillowed basalt. Conglomerate boulders and pebbles of metabasalt and metadacite are likely derived from erosion of the Roebourne and Whundo Groups and the BIF and chert are most likely derived from the underlying Cleaverville Formation. Geochemistry is briefly discussed. See also  p29 tbl 5, p39, p41, p43, p46-p47, p49-p53, p62, p75.|c. 3015-2991 Ma|Whim Creek Group||Unconformably overlies the Cundaline Formation and the Cleaverville Formation. Overlain by the Red Hill Volcanics. Intruded by the Mons Cupri Dacite Member.|Vesicular basalt and basaltic andesite, locally porphyritic, volcaniclastic and siliciclastic sedimentary rocks; metamorphosed.|
29116|Warambie Basalt|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Whim Creek Basin.||Whim Creek Group|||Vesicular basalt and basaltic andesite, locally porphyritic, and volcaniclastic and siliciclastic sedimentary rocks; metamorphosed.|
29116|Warambie Basalt|72251|5|Briefly described|p54|Mesoarchean|Mesoarchean|Geological province: West Pilbara Superterrane, Pilbara Craton.||Unit of Whim Creek Group.||Overlain by Red Hill Volcanics. Underlain unconformably by Cleaverville Formation. Correlable to Constantine Sandstone.||
29116|Warambie Basalt|72668|4|Described|p4, p14|||West Pilbara Superterrane. Geochemical data show incompatible trace element enrichment relative to tholeiitic arc basalts and a withinplae compositional signature.||Whim Creek Group||Overlain by the Red Hill Volcanics. Coeval with the Mons Cupri Dacite Member.|Basalt, andesite and transitional alkaline basalt.|
77242|Waratjarra suite|66256|5|Briefly described|p8, p18 Fig.14, p24-32, see comments|Stenian|Stenian|Age: late Musgravian. In western part of Mamutjarra Zone, straddling boundary with southeastern part of Tjuni Purlka Tectonic Zone. Systematic compositional variation that parallels northwest trend of major shear zones. Geochemistry provided. SHRIMP crystallization age range. See also p34-38, p41, p43-44, p53-54 App.1, p64-65 App.3.|1162+/-16 Ma to 1148+/-6 Ma (GSWA).|Pitjantjatjara Supersuite|||Granite.|11-JAN-17
77242|Waratjarra suite|67375|6|Mentioned|p25 Fig.17, p26 Fig.19. |Mesoproterozoic|Mesoproterozoic|A-type. Within-plate, Yb-enriched granite. Late Musgrave Orogeny.||Unit in Pitjantjatjara Supersuite.||||
77242|Waratjarra suite|67553|6|Mentioned|p27-28,33|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province, North Australian Craton. Late Musgravian granite.||Unit of Pitjantjatjara Supersuite.||||
77242|Waratjarra suite|69091|5|Briefly described|p64 Fig.4.10|||late Musgravian granite||Pitjantjatjara Supersuite||||
77242|Waratjarra suite|69729|5|Briefly described|p74 Fig.7, p77-78|||Geochemistry plots.||Pitjantjatjara Supersuite.|||A-type granites.|
79003|Warbadoo Tonalite|70226|5|Briefly described|Map legend.|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Carton.|c. 2743 Ma (Fletcher and McNaughton, 2002).|Rothsay Suite.|||Sheets of granite, granodiorite and tonalite, aplitic dykes, pegmatite sheets, monzogranite; metamorphosed. Also, migmatitic or hornblende tonalite, interlayered monzogranitic augen gneiss and granodiorite schist.|16-DEC-15
79003|Warbadoo Tonalite|70796|4|Described|100k_geologyl_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, Yalgoo100_2241_stratig.pdf. Numerous additional lithologies are discussed.|ca 2743 Ma (inferred)|Rothsay Suite|||Metamorphosed granitic sheets, aplitic dykes, pegmatite sheets and muscovite rich pegmatite sheets.|
79003|Warbadoo Tonalite|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.|2743+\-4 Ma|Unit of Rothsay Suite.|||Equigranular monzogranite; metagranitic to metatonalitic schist, locally as intrusive sheets into country rocks; migmatitic and hornblende tonalite; interlayered monzogranitic augen gneiss and granodiorite schist.|
78455|Warlawurru Supersuite|69729|5|Briefly described|p64, p70-71|Mesoproterozoic|Mesoproterozoic|Exposed basement in west Musgrave Province. Has a distinctive magnetic pattern. Also appears as Warlawurra Supersuite in p70 (text).|c.1575 Ma (GSWA 201304).||||Granulite-facies metagranites; gneissic biotite granite.|
78455|Warlawurru Supersuite|70084|4|Described|p220-221,223-225|Calymmian|Statherian|Geological province: Musgrave Province, Paterson Orogen. Associated with major crust formation and juvenile addition in the Paterson Orogen and Madura Province. Correlable with Krackatinny Supersuite in the Rudall Province. Oldest exposed basement rocks in the Madura Province; with 1600-1550 Ma protolith ages (Howard et al., 2015; Camacho and Fanning, 1995; Edgoose et al., 2004). Lies within a single, narrow, Nd and Hf-isotopic evolution band with TDM2 values within a range of 2.2-1.6 Ga, together with the Pitjantjatjara, Papulankutja and Wankanki supersuites, reflecting reworking of juvenile crust between ca. 2.0 and 1.6 Ga (Kirkland et al., 2013a).|c. 1575 Ma||||Rare calc-alkaline orthogneiss and granulites.|
78455|Warlawurru Supersuite|70619|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province.|c. 1600 Ma||||Metasyenogranite and gneiss.|
78455|Warlawurru Supersuite|70763|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province.|c.1600 Ma.||||Strongly foliated to gneissic biotite(-hornblende) metasyenogranite; garnet-bearing; commonly migmatitic.|
78455|Warlawurru Supersuite|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Proterozoic|Geological province: Paterson Orogen, Musgrave Province. Exposed in the Wanarn area between the Mitika Fault to the south and the Woodroffe Thrust to the north. Limited exposure Warlawurru Supersuite in the west Musgrave Provincedeu to N-directed thrusting during the Neoproterozoic Petermann Orogeny (Howard et al., 2015; Quentin de Gromard et al., in prep.). Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma); Musgrave Orogeny (1220-1150 Ma); Mount West Orogeny (1345-1293 Ma). Sample GSWA 201303 (metasyenogranite) yielded an interpreted (weighted mean 207Pb*/206Pb*) magmatic crystallisation age of 1583+\-10 Ma, and a high-grade metamorphic date (207Pb*/206Pb*) of 1179+\-11 Ma. Sample GSWA 208455 (foliated metasyenogranite) yielded an interpreted (weighted mean 207Pb*/206Pb*) magmatic crystallisation age of 1594+\-14 Ma, and a (207Pb*/206Pb*) metamorphic event at 1166+\-5 Ma. Sample GSWA 208502 (foliated metasyenogranite) yielded an interpreted (weighted mean 207Pb*/206Pb*) magmatic crystallisation age of 1607+\-11 Ma, and a (207Pb*/206Pb*) metamorphic event at 1185+\-11 Ma. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 2_5m_interpgeop15_lut.csv.|1607-1583 Ma (inferred)|||Overlain unconformably by Bentley Supergroup.|Strongly foliated to gneissic biotite(--hornblende) metasyenogranite; garnet-bearing; commonly migmatitic|
78455|Warlawurru Supersuite|70826|6|Mentioned|p2, p10|Mesoproterozoic|Mesoproterozoic|Musgrave Province. ||||Broadly coeval with Waldburg and Narimbunna  Dolerite Suites.||20-MAY-20
78455|Warlawurru Supersuite|70831|5|Briefly described|p1-p7, p13-p15, p20, p22, p25|Calymmian|Statherian|Musgrave Province. Average mineralogy is discussed. Petrography of constituent samples is discussed.|c. 1607-1583 Ma||||Strongly foliated to gneissic, garnet-bearing, biotite-hornblende metasyenogranites. This supersuite is commonly migmatitic and contains locally abundant pegmatite veins.|
78455|Warlawurru Supersuite|70839|5|Briefly described|p326-327,339|Calymmian|Calymmian|Geological province: Musgrave Province. [Misspelt Warlawurra Supersuite on p339]. Observed as localised outcrops of granulite facies metagranites.|c. 1575 Ma|||||
78455|Warlawurru Supersuite|71088|6|Mentioned|p4|||West Musgrave Province.|c. 1575 Ma|||||
78455|Warlawurru Supersuite|71169|5|Briefly described|p78|Calymmian|Calymmian|Musgrave Province. |1607-1583 Ma||||Calc-alkaline granitic gneiss and granulite.|
78455|Warlawurru Supersuite|71210|6|Mentioned|p5-p6|||Musgrave Province.|c. 1575 Ma|||||
78455|Warlawurru Supersuite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Proterozoic|Geological Province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Exposed in the Wanarn area between the Mitika Fault to the south and the Woodroffe Thrust to the north. Limited exposure of the Warlawurru Supersuite in the west Musgrave Province is a result of N-directed thrusting during Petermann Orogeny (Howard et al., 2015; Quentin de Gromard et al., in prep.). Sample GSWA 201304 (metasyenogranite) yielded weighted mean 207Pb/206Pb dates of 1583+\-10 and 1179+\-11 Ma, interpreted as magmatic crystallisation age of the syenogranite, and age of metamorphism respectively. Sample GSWA 208455 (bt-hbl metasyenogranite) yielded a weighted mean 207Pb/206Pb age of 1594+\-14 Ma, interpreted as magmatic crystallisation age of the syenogranite. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|1607-1542 Ma (inferred)||||Strongly foliated to gneissic biotite(-hornblende) metasyenogranite; garnet-bearing; commonly migmatitic|
78455|Warlawurru Supersuite|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1594+/-14 Ma (crystallisation: U-Pb zircon SHRIMP)||||Medium-grained, equigranular, hornblende-porphyritic, garnet-bearing foliated metasyenogranite; strongly foliated inequigranular garnetiferous metamonzogranite to metasyenogranite.|
78455|Warlawurru Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Proterozoic|Musgrave Province, Paterson Orogen.|||||Strongly foliated to gneissic biotite(-hornblende) metasyenogranite; garnet-bearing; commonly migmatitic.|
78455|Warlawurru Supersuite|72094|5|Briefly described|p2, p3, p6, 8, 11, 13, 14, p15-16|Calymmian|Statherian|Musgrave Province.  Oldest known rocks of the west Musgrave Province. Underwent UHT metamorphism during Musgrave Orogeny. Summary table of zircon geochronology on p8 Table 1 showing magmatic  crystallisation ages ranging from 1607+/-11 Ma to 1583+/-10 Ma.|1607, 1542 Ma mag. cryst.|||Tectonically interleaved with Kunmarnara Group along with Pitjantjatjara Supersuite.|Migmatitic orthogneiss.|
78455|Warlawurru Supersuite|73346|6|Mentioned|p2, p5|Calymmian|Statherian|Musgrave Province.|1607-1542 Ma||||Granulite facies metagranite.|
78455|Warlawurru Supersuite|73437|5|Briefly described|p151, p153|Mesoproterozoic|Mesoproterozoic|Musgrave Province, western. Poorly exposed.|1607-1542 Ma||||Migmatic orthogneiss.|
80581|Warmun Dolerite|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|North Australian Craton. Typically NW-trending dykes crosscutting the Central and Western Lamboo Provinces.|||||Dolerite dykes.|
80795|Warnbro Megasequence|71958|5|Briefly described|p40-p41, p45-p46, p51, p61|Aptian|Valanginian|Vlaming Sub-basin. Sequence stratigraphy. Major deltaic to shallow marine succession. Intersected in all wells from the Sub-basin.|||Includes the South Perth Supersequence and the Leederville Supersequence.|||
80130|Waroonga Gneiss|71212|5|Briefly described|p73, 61, 72, 76, 77, 88, 90|||Yilgarn Craton. Outcrop characteristics and distribution discussed. See also  p92, p140, p249, App B tbl B1, tbl B2. See also Waroonga Granite Gneiss p46.||||Overlies the Scotty Creek Metasediments.|Quartz-albite-orthoclase leucogranites, garnetiferous luecogranite and porphyritic monzogranite.|26-SEP-17
80130|Waroonga Gneiss|73151|6|Mentioned|p4|||Yilgarn Craton. Waroonga Shear Zone, western margin.|||||Granulite facies peak metamorphic conditions.|
80130|Waroonga Gneiss|73596|6|Mentioned|p1152, 1157-1158, 1160|||Waroonga Domain, Agnew-Wiluna Greenstone Belt.||||Is faulted against Scotty Creek Formation (to the E).||
37219|Waroonga gneiss|23989|6|Mentioned|p76|||Geological Province: Yilgarn Craton||||||
37219|Waroonga gneiss|69586|5|Briefly described|p13-14||||||||Biotite-rich granodiorite gneisses, generally deeply weathered, and sheared leucogranitic dykes. Contains large amphibolite xenoliths.|
37219|Waroonga gneiss|71310|5|Briefly described|p777|||Located immediately W of Jones Creek Conglomerate. Minimum age from intrusive granodiorite.|>2655 +/- 4 Ma (SHRIMP U-Pb; Dunphy et al. 2003).||||Metatonalite.|
24079|Waroongunyah Formation|22907|5|Briefly described|41|||||||||
24079|Waroongunyah Formation|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Of Tarcunyah Group, Officer Basin.||||||
24079|Waroongunyah Formation|23583|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Tarcunyah Group.||||||
24079|Waroongunyah Formation|23585|4|Described|p21|Neoproterozoic|Neoproterozoic|Of Tarcunyah Group.||||||
24079|Waroongunyah Formation|23590|3|Fully described|p11|||Of Tarcunyah Group. Underlain by Googhenama Formation. Geological Province: Officer Basin. Max. thickness: ~600 m.||||||11-JUL-13
24079|Waroongunyah Formation|23594|4|Described|p22|Neoproterozoic|Mesoproterozoic|Of Tarcunyah Group. Overlain by Brownrigg Sandstone. Underlain by Googhenama Formation. Geol. prov: Bangemall Basin. Max. thickness: >300 m.||||||24-JUL-07
24079|Waroongunyah Formation|23745|4|Described|p17|Neoproterozoic|Mesoproterozoic|See also page 7 Fig 5. Of Tarcunyah Group. Geological Province: Yeneena Basin. Max. thickness: 300 m.||||||
24079|Waroongunyah Formation|23746|4|Described|p25|Neoproterozoic|Mesoproterozoic|Of Tarcunyah Group. Max. thickness: 400 m.||||||
24079|Waroongunyah Formation|23760|4|Described|p28|Proterozoic|Proterozoic|Of Tarcunyah Group. Geological Province: Officer Basin.||||||
24079|Waroongunyah Formation|41669|2|Defined|Table 5|Precambrian?||||||||
24079|Waroongunyah Formation|42352|6|Mentioned|p29|||Part of Yeneena Group||||||
24079|Waroongunyah Formation|43055|4|Described|p27, Table 4|||Of the Yeneena Group.||||||24-JUL-07
24079|Waroongunyah Formation|43056|5|Briefly described|Map Legend|||Of the Yeneena Group.||||||24-JUL-07
24079|Waroongunyah Formation|43847|5|Briefly described|Map Legend||Proterozoic|||||||
24079|Waroongunyah Formation|44111|6|Mentioned|p58 and Fig. 2|||Of Tarcunyah Group. Includes evaporites, stromatolitic carbonates and red beds.||||||
24079|Waroongunyah Formation|44139|5|Briefly described|p277-280|Neoproterozoic|Neoproterozoic| (Williams 1989). 250 m. Dolomite, shale, siltstone, sandstone. Contains stromatolites. Western zone of Yeneena Basin. Overlies Googhenama Formation. Incorporates former Wandy Wandy Shale rocks.| | ||||06-MAR-18
24079|Waroongunyah Formation|44189|5|Briefly described|Map legend||Proterozoic|||||||
24079|Waroongunyah Formation|44190|5|Briefly described|Map Legend||Proterozoic|||||||
24079|Waroongunyah Formation|44831|5|Briefly described|Map Legend||Proterozoic|||||||
24079|Waroongunyah Formation|50008|5|Briefly described|p46 Fig.3|Neoproterozoic||Of Tarcunyah Group. Geological Province: Officer Basin.||||||
24079|Waroongunyah Formation|50544|4|Described|p58|Neoproterozoic|Neoproterozoic|Of the Tarcunyah Group.  Overlies the Googhenama Formation; also unconformable over the Kyleena Formation.  Max. thickness: >700m.  Transgressive shallow marine succession.||||||22-APR-16
24079|Waroongunyah Formation|50555|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Tarcunyah Group.  Interbedded dolomite, sandstone, siltstone and shale.   Age: c.800Ma.  Geological Province: Officer Basin.||||||24-JUL-07
24079|Waroongunyah Formation|60470|5|Briefly described|p4 Fig. 2|Neoproterozoic|Neoproterozoic|in Officer Basin, of Tarcunyah Group. Stromatolitic carbonate units, red beds, siltstone, shale, and evaporite units||||||
24079|Waroongunyah Formation|62453|3|Fully described|p5 Fig. 3, 65, 16|Cryogenian|Cryogenian|Geological Province: Paterson Orogen. Of the Tarcunyah Group. Conformably overlies Googhenama Formation. Correlates with Waters Formation. Thickness: ~600m. Dolomite, siltstone, shale, sandstone. Type section 8.5 km northeast of Canning Well on Balfour Downs, at MGA Zone 51, 333500E 7529400N.||||||30-AUG-18
24079|Waroongunyah Formation|63417|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Tarcunyah Group. Geological Province: Officer Basin (Centralia Superbasin). Dolostone, siltstone, shale and sandstone; in part stromatolitic; evaporite pseudomorphs.||||||
24079|Waroongunyah Formation|64580|6|Mentioned|map legend|||Of Tarcunyah Group.||||||15-DEC-08
24079|Waroongunyah Formation|64777|5|Briefly described|p3 Fig.4 |Neoproterozoic|Neoproterozoic|||Of the Tarcunyah Group||||
24079|Waroongunyah Formation|65454|4|Described|p7 Fig.3, p10, p30 Fig.A1b|Cryogenian|Cryogenian|Of Tarcunyah Group. Overlies Googhenama Formation. Overlain by Brownrigg Sandstone. Laminated to massive dolomite, minor stromatolitic dolomite, dolomitic siltstone, shale and siltstone. ||||||
24079|Waroongunyah Formation|65725|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Tarcunyah Group. Underlain by Googhenama Formation. Overlain by Brownrigg Sandstone. Shale, siltstone, sandstone and dolomite. Age <1070 Ma. Province: Officer Basin (Centralian Superbasin)||||||26-FEB-13
24079|Waroongunyah Formation|65826|4|Described|p1, p11. |Neoproterozoic|Neoproterozoic|A transgressive shallow-marine sequence deposited shorewards of carbonate build-ups. About 600 m thick.||Unit in Tarcunyah Group.||Conformably overlies Googhenama Formation.|Rarely exposed dolomite, massive to laminated, locally stromatolitic, silicified, sandy or oolitic; interbedded with pink to grey-white siltstone and shale, and thin beds of brown, fine-grained sandstone containing scattered halite pseudomorphs.|23-MAY-16
24079|Waroongunyah Formation|67202|4|Described|p64-66, p117, p125, p231-232, p234-237|Neoproterozoic|Neoproterozoic|NW Officer Basin. 300m thick. Transgressive shallow-marine deposits. Correlation with Waltha Woora Formation proposed, based on common stromatolite taxa. Conductance image.||Tarcunyah Group.||Thin-bedded, laminated, multicoloured dolomite and brown to grey, calcareous shale and siltstone; thin beds of medium to coarse-grained dolomitic sandstone, wacke and pebbly dolomite.|Calcareous siltstone, shale, dolomite and fine- to medium-grained sandstone.|15-FEB-18
24079|Waroongunyah Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|NW Paterson Orogen.||Tarcunyah Group.||||
24079|Waroongunyah Formation|69167|4|Described|geologyp_lut.csv|Neoproterozoic|Neoproterozoic|||Tarcunyah Group|||Bedded to laminated dolomite and stromatolitic dolomite, siltstone, shale; sandstone; evaporite pseudomorphs.|
24079|Waroongunyah Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|Neoproterozoic|Neoproterozoic|||Unit of Tarcunyah Group.||||
24079|Waroongunyah Formation|69590|4|Described|GEOL_LUT_CSV files|Cryogenian|Neoproterozoic|Of Gibson Sub-basin, Officer Basin (Phase 1), Centralian Superbasin. Events: Delamarian Orogeny; Paterson Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|1000-635 Ma (Inferred)|Unit of Tarcunyah Group.|||Bedded to laminated dolomite and stromatolitic dolomite; sandstone, siltstone, shale, evaporite pseudomorphs.|
24079|Waroongunyah Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone, crystalline dolostone/dolomite|
24079|Waroongunyah Formation|72034|5|Briefly described|500k_interpgeop16_lut|Cryogenian|Tonian|Gibson Sub-basin, Officer Basin (Phase 1).||Tarcunyah Group|||Dolomite, in part stromatolitic, siltstone, shale; sandstone; evaporite pseudomorphs.|
36897|Warri Warri Member|23570|3|Fully described|p149|Archean|Archean|See also  p240 App. 1.  Of Hardey Formation.   Overlain by Tanguin Member; underlain by Koongaling Volcanic Member.   Geological Province: Pilbara Craton||||||07-NOV-08
36897|Warri Warri Member|23594|3|Fully described|p13|Archean|Archean|Age: 2760+/-10 Ma (SHRIMP U-Pb zircon). Of Hardey Formation. Overlying unit Kylena Basalt. Underlying unit Koongaling Volcanic Member. Hamersley Basin.||||||07-NOV-08
36897|Warri Warri Member|23746|5|Briefly described|p16|||Of Hardey Formation. Geological Province: Hamersley Basin.||||||
36897|Warri Warri Member|24185|5|Briefly described|p745 Tb.4|Archean|Archean|Parent: Koongaling Volcanics. Geological Province: Pilbara Craton.||||||07-NOV-08
36897|Warri Warri Member|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Hardey Formation|||Mixed felsic (rhyolitic) and mafic lavas. Volcaniclastic siliciclastic rocks, felsic volcanic breccia and agglomerate. Oligomictic conglomerate; sandstone.|
36897|Warri Warri Member|69590|4|Described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Of Northeast Pilbara Sub-basin; Marble Bar Sub-basin, Fortescue Basin. Events: Pilbara Craton breakup.|2766-2749 Ma (inferred)|Unit of Hardey Formation.|||Epiclastic sandstone, felsic volcanic breccia and agglomerate, mixed felsic and mafic lavas and rocks, rhyolite, oligomictic conglomerate with felsic volcanic clasts, volcaniclastic siliciclastic rocks.|
29121|Warrie Member|23354|5|Briefly described|316|||||||||
29121|Warrie Member|23570|4|Described|p129, p239 Appendix 1|||See also Warrie Shale Member.   Max. thickness: 82m.  Overlies the Woodiana Sandstone Member; underlies the Roy Hill Shale Member.||||||12-DEC-12
29121|Warrie Member|23575|5|Briefly described|Map Legend|Archean|Archean|Of Hardey Formation.||||||07-NOV-08
29121|Warrie Member|24573|6|Mentioned|p682|||Geological Province: Pilbara Craton||||||
29121|Warrie Member|34128|6|Mentioned|p17|||||||||
29121|Warrie Member|34129|6|Mentioned|p57|||Proterozoic||||||
29121|Warrie Member|35059|6|Mentioned|p205|||||||||
29121|Warrie Member|35260|5|Briefly described|Table 1|||||||||
29121|Warrie Member|36882|6|Mentioned|p124|||||||||
29121|Warrie Member|37460|3|Fully described|Table 3.I|||||||||
29121|Warrie Member|39030|6|Mentioned|p3|||||||||
29121|Warrie Member|39697|5|Briefly described|p123|||||||||
29121|Warrie Member|43595|6|Mentioned|Table 2-29,p219|||||||||
29121|Warrie Member|44152|5|Briefly described|p173-174, p176 Fig.2-154|||MacLeod and de la Hunty (1966).||Jeerinah Formation||Overlies Woodiana Sandstone Member. Is overlain by Roy Hill Shale Member.|Shale, chert (locally ferruginous), mudstone and dolomite.|
29121|Warrie Member|44477|4|Described|p.9, Table 1||Proterozoic|SF/50-6.||||||
29121|Warrie Member|44478|14|Not recorded|map legend||Proterozoic|||||||
29121|Warrie Member|44501|14|Not recorded|p.7, Table 4, map||Paleoproterozoic|(ref. to MacLeod and de la Hunty 1966). (F50-7). Lower Proterozoic.||||||07-NOV-08
29121|Warrie Member|44502|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
29121|Warrie Member|44503|2|Defined|p.12,18,Tb.2, map||Paleoproterozoic|Unit of Jeerinah Formation. Lower Proterozoic. Roy Hill Sheet. (F50-12).||||||07-NOV-08
29121|Warrie Member|44504|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
29121|Warrie Member|60373|4|Described|p145 Tb. 1|Archean|Archean|Of Jeerinah Formation. Overlain by Roy Hill Shale Member, underlain by Woodiana Sandstone Member.||||||
29121|Warrie Member|62579|5|Briefly described|p116|Archean|Archean|Middle unit of Jeerinah Formation (Fortescue Group, Mount Bruce Supergroup). Geological Province: Pilbara Craton. Carbonate-rich rock.||||||07-NOV-08
29121|Warrie Member|66685|5|Briefly described|p217 Fig.2|Archean|Archean|||Jeerinah Formation||Overlies the Woodiana Member, underlies the Roy Hill Member.|Basalt.|
29121|Warrie Member|67201|5|Briefly described|p29 Fig.15|||Northern Fortescue Basin, Northeast and Northwest Pilbara Sub-basins.||Jeerinah Formation||||
29121|Warrie Member|67229|6|Mentioned|p3 Fig.2|||MacLeod and de la Hunty (1965).||Jeerinah Formation.||||
29121|Warrie Member|68056|6|Mentioned|p185|Archean|Archean|||||||
29121|Warrie Member|69301|5|Briefly described|p18 Fig.7|||Pilbara Craton. Fortescue Basin. Northeast Pilbara Sub-basin, Northwest Pilbara Sub-basin, Sequence 4. ||Jeerinah Formation||||
78997|Warriedar Suite|70226|5|Briefly described|map legends|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Carton.|2801-2793 Ma|Annean Supersuite.|Noongal, Wadgingarra, Olive Queen Gabbros.||Mainly metamorphosed mafic/ultramafic rocks.|16-DEC-15
78997|Warriedar Suite|70419|6|Mentioned|p2|||Murchison Domain, Youanmi Terrane, Yilgarn Craton. Mafic-ultramafic intrusives.||||||
78997|Warriedar Suite|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton. Seven facies associations are mapped separately.|2801-2793 Ma.|Annean Supersuite.|||Peridotite and pyroxenite, local cumulate textures, serpentinized; ultramafic schist; gabbro, dolerite, locally interlayered; weakly schistose metagabbro. All metamorphosed.|
78997|Warriedar Suite|70796|5|Briefly described|100k_geologyl_lut.csv|Neoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 198294.1.pdf, Badja100_2240_stratig.pdf. Numerous additional lithologies are discussed.|ca 28012793 Ma (inferred)|Annean Supersuite|Includes the Olive Queen Gabbro, Noongal Gabbro and the Wadgingarra Gabbro.||Metagabbro; locally with layers of metaleucogabbro, metagabbronorite, metadolerite and minor metapyroxenite; includes amphiboleporphyroblastic metagabbro and metadolerite.|
78997|Warriedar Suite|70830|5|Briefly described|p2, p5, p9, p27-p28, p57-p58|Neoarchean|Neoarchean|Murchison Domain. |c. 2795 Ma|Annean Supersuite|Includes the Ninghan Gabbro.|||
78997|Warriedar Suite|71168|6|Mentioned|p19 fig 11|||Youanmi Terrane, Yilgarn Craton. Youanmi Terrane, Yilgarn Craton.||||||28-AUG-20
78997|Warriedar Suite|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). Previous geochronological analyses yielded a volcaniclastic metasandstone maximum depositional age of 2826+\-7 Ma (Lu et al., 2016a) and a metadacite maximum crystallisation age of 2801+\-5 Ma (Lu et al., 2016b). Sample GSWA 198294 (metamorphosed qtz diorite) yielded a weighted mean 207Pb/206Pb date of 2801 ¿ 6 Ma, interpreted as the magmatic crystallization age of the quartz diorite. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.|2801-2793 Ma (inferred)|Unit of Annean Supersuite.|Includes Noongal Gabbro, Olive Queen Gabbro, Wadgingarra Gabbro.||Basal pyroxenite to pyroxene peridotite, typically showing cumulate textures; metagabbro interlayered with metaleucogabbro, metagabbronorite, metadolerite and metapyroxenite; gabbroic schist, gabbro, dolerite, serpentinite, ultramafic schist.|
78997|Warriedar Suite|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|2801-2792 Ma.|Annean Supersuite.|||Pyroxenite to pyroxene peridotite, gabbro-leucogabbro, metadolerite, metamorphosed gabbro, leucogabbro, gabbronorite, dolerite and pegmatitic gabbro.|
78997|Warriedar Suite|71272|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Six facies are mapped separately.|2801-2793 Ma.|Annean Supersuite.|||Pyroxenite to pyroxene peridotite; metamorphosed gabbro, dolerite, leucogabbro, gabbronorite; ultramafic talc-tremolite-serpentine-magnetite schist; serpentinite; peridotite with local relict cumulate textures.|
78997|Warriedar Suite|71809|5|Briefly described|map legend|Archean|Archean|Yilgarn Craton|||Includes Ninghan Gabbro.|||
78997|Warriedar Suite|72389|5|Briefly described|Map Legend|Archean|Archean|Gabanintha 1:100k map sheet 2644. Includes numerous unnamed constituents.||Annean Supersuite|||Basal pyroxenite to pyroxene peridotite, typically showing cumulate textures; gabbro-leucogabbro in central to upper parts, locally layered and with doleritic to granophyric top contacts; metamorphosed.|
78997|Warriedar Suite|72494|5|Briefly described|p14, 16, 18, 22, 28|||Murchison Domain, Youanmi Terrane, Yilgarn Craton. Geochemistry plots. Also appears as Warriedar intrusive suite (p16), Warriedar suite (p18), Warriedar Intrusive Suite (p22, 28).|~2792 Ma.||||Peridotite to gabbro and dolerite. Numerous small intrusions with larger mafic-ultramafic complexes extending to c.10 km.|
36971|Warrigal Gneiss|23485|4|Described|p12|Archean|Archean|Age: c.2700Ma. Geological Province: Yilgarn Craton.||||||07-NOV-08
36971|Warrigal Gneiss|23486|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
36971|Warrigal Gneiss|23780|5|Briefly described|p31|Archean|Archean|||||||07-NOV-08
36971|Warrigal Gneiss|23781|4|Described|p36|Paleoproterozoic|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
36971|Warrigal Gneiss|24544|5|Briefly described|p8, 17-18|Archean|Archean|Well foliated to banded granites, biotite monzogranite.||||||07-NOV-08
36971|Warrigal Gneiss|50218|5|Briefly described|p240 Fig.2, p244|Archean|Archean|Pegmatite banded granitic gneiss. Age: 2700-2600Ma. Geological Province: Yilgarn Craton. See also p248.||||||07-FEB-11
36971|Warrigal Gneiss|50219|5|Briefly described|p260 Fig. 2|||Geological Province: Yilgarn Craton.||||||07-FEB-11
36971|Warrigal Gneiss|50220|5|Briefly described|p281 Fig.1|Archean|Archean|Granitic gneiss. Age: 2700-2600 Ma. See also p292 Tb.2||||||07-NOV-08
36971|Warrigal Gneiss|63866|5|Briefly described|p157-p158|Neoarchean|Neoarchean|Erabiddy Shear Zone. SHRIMP U-Pb ages derived from Nelson, 2000 and Occhipinti et al., 2001.|2700-2600 Ma (SHRIMP U-Pb)||||Well-foliated to banded, interleaved mesocratic and leucocratic granite phases.|
36971|Warrigal Gneiss|64580|4|Described|map legend|Proterozoic|Archean|Foliated to gneissose, even-textured to sparsely porphyritic metamonzogranite; locally contains sheets and pods of amphibolite; cut by c. 1800 Ma pegmatite dykes. Deformation is Paleoproterozoic.||||||15-DEC-08
36971|Warrigal Gneiss|65692|6|Mentioned|p29|Archean|Archean|Glenburgh Terrane. Hf values briefly mentioned to support the suggestion of a possible source for some Earaheedy Basin sediments.||||||
36971|Warrigal Gneiss|66299|4|Described|p49, p95, p114.|Neoarchean|Neoarchean|Forms fault-bounded inliers in Camel Hills Metamorphics. Gneissic fabric is determined by alternating leucocratic and mesocratic layers.|c.2758 Ma to c.2585 Ma.|||Faulted against Camel Hills Metamorphics.|Foliated to gneissose, even-textured to sparsely porphyritic metamonzogranite; contains sheets and pods of amphibolite.|
36971|Warrigal Gneiss|67247|5|Briefly described|Map legend.|Archean|Archean|Narryer Terrane, Yilgarn Craton.|2758 - 2585 Ma.||||Foliated to gneissic, even-textured to sparsely-porphyritic metamonzogranite; locally contains sheets and pods of amphibolite; cut by c.1800 Ma pegmatite dykes; deformation is Paleoproterozoic.|
36971|Warrigal Gneiss|67843|6|Mentioned|p12.|Archean|Archean|Contains gneissic fabric defined by alternating mesocratic and leucocratic layers.||||||
36971|Warrigal Gneiss|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv|Proterozoic|Archean||||||Foliated to gneissose, even-textured to sparsely porphyritic metamonzogranite; locally contains sheets and pods of amphibolite; cut by c. 1800 Ma pegmatite dykes. Deformation is Paleoproterozoic|
36971|Warrigal Gneiss|69028|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Narryer Terrane.|2758-2585 Ma||||Foliated to gneissic, even-textured to sparsely porphyritic metamonzogranite; locally contains sheets and pods of amphibolite; cut by c. 1800 Ma pegmatite dykes; deformation is Paleoproterozoic.|06-MAY-14
36971|Warrigal Gneiss|69080|6|Mentioned|p684|||Yilgarn Craton.|||||Foliated to gneissic, even-textured to sparsely porphyritic metamonzogranite.|
36971|Warrigal Gneiss|69166|5|Briefly described|geologyp_lut.csv|Neoarchean|Neoarchean||||||Foliated to gneissic, even-textured to sparsely porphyritic metamonzogranite; locally contains sheets and pods of amphibolite; cut by c. 1800 Ma pegmatite dykes; deformation is Paleoproterozoic|
36971|Warrigal Gneiss|69387|6|Mentioned|p3, p13|||Yilgarn Craton.||||||
36971|Warrigal Gneiss|69583|5|Briefly described|p130, Plate 3|Archean|Archean|Narryer Terrane. Deformed in the Paleoproterozoic.|2758-2585 Ma.|Yarlarweelor Gneiss Complex.|||Foliated to gneissic, even-textured to sparsely porphyritic metamonzogranite; locally contains sheets and pods of amphibolite.|
36971|Warrigal Gneiss|70795|4|Described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Also 2_5m_interpgeop15_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv|2758-2585 Ma||||Foliated to gneissic, even-textured to sparsely porphyritic metamonzogranite; locally contains sheets and pods of amphibolite; cut by pegmatite dykes.|
36971|Warrigal Gneiss|70796|4|Described|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean|Affected by the Capricorn Orogeny (1817  1772 Ma); Yilgarn Craton events (4000  2600 Ma). See also 500k_interpgeop14_lut.csv.|2758 +/ 4 Ma to 2585 +/ 8 Ma (isotopic)||||Foliated to gneissic, eventextured to sparsely porphyritic metamonzogranite; locally contains sheets and pods of amphibolite; cut by c. 1800 Ma pegmatite dykes; deformation is Paleoproterozoic|
36971|Warrigal Gneiss|70826|6|Mentioned|p9|Neoarchean|Neoarchean|Narryer Terrane.||||||
36971|Warrigal Gneiss|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||felsic gneiss|
36971|Warrigal Gneiss|71269|5|Briefly described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Narryer Terrane, West Australian Craton. Of Yarlarweelor Gneiss Complex. Events: Capricorn Orogeny (1817-1772 Ma); Yilgarn Craton events (4000-2600 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv.|2758+\-4 Ma; 2585+\-8 Ma||||Foliated to gneissic, even-textured to sparsely porphyritic metamonzogranite; locally contains sheets and pods of amphibolite; cut by c. 1800 Ma pegmatite dykes; deformation is Paleoproterozoic|
36971|Warrigal Gneiss|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Narryer Terrane.|Max age 2758+/-4 Ma, min 2585+/-8 Ma.||||Foliated to gneissic, even-textured to sparsely porphyritic metamonzogranite; locally contains sheets and pods of amphibolite; cut by c. 1800 Ma pegmatite dykes; deformation is Paleoproterozoic.|
36971|Warrigal Gneiss|72259|6|Mentioned|p3, App. Tb.B|Neoarchean|Archean||ca. 2600 Ma||||Includes granitic gneiss.|
36896|Warroo Hill Member|23570|4|Described|p151|Archean|Archean|See also p240 App. 1.  Formerly assigned to the Bangemall Group. Of Hardey Formation. Overlain by the Tarcunyah Group; underlain by the Tanguin Member.   Thickness:>1000m.   Geological Province: Pilbara Craton||||||07-NOV-08
36896|Warroo Hill Member|23594|5|Briefly described|p9 Fig 6|Archean|Archean|Of Hardey Formation. Hamersley Basin.||||||07-NOV-08
36896|Warroo Hill Member|23745|4|Described|p11|Archean|Archean|See also page 7 Fig 5. Of Hardey Formation.||||||07-NOV-08
36896|Warroo Hill Member|23746|4|Described|p15|Archean|Archean|Of Hardey Formation. Geological Province: Hamersley Basin. Max. thickness: >1000 m.||||||07-NOV-08
36896|Warroo Hill Member|50544|5|Briefly described|p47|Archean|Archean|Epiclastic compnent of the Hardey Formation - mica-rich pelitic and psammitic schist and semischist.  Overlies the Koongaling Volcanic Member (Gregory Range Inlier).||||||07-NOV-08
36896|Warroo Hill Member|50555|5|Briefly described|Map legend|Archean|Archean|Of Hardey Formation (Fortescue Group, Mount Bruce Supergroup) -in Gregory Range area.   Metasandstone, quartzite, and metasiltstone.  Geol. Prov: Hamersley Basin.||||||07-NOV-08
36896|Warroo Hill Member|67202|5|Briefly described|p236|Archean|Archean|Potential trap for uranium.||Hardey Formation|||Metamorphosed fine- to coarse-grained clastic rock, tuff, and mafic rock: metasandstone, metaconglomerate, metasiltstone, quartzite, quartz-mica schist, phyllite, slate, metadolomite, metabasalt and metabasaltic andesite with local amygdules.|15-FEB-18
36896|Warroo Hill Member|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Hardey Formation|||Metabasalt and metabasaltic andesite; local amygdales, metadolomite, pelite, quartz-mica schist, phyllite, slate. Metasandstone, metaconglomerate, metasiltstone and quartzite.|
36896|Warroo Hill Member|69590|4|Described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Of Northeast Pilbara Sub-basin; Marble Bar Sub-basin, Fortescue Basin. Events: Pilbara Craton breakup.|2766-2749 Ma (inferred)|Unit of Hardey Formation.|||Metabasalt and metabasaltic andesite; local amygdales; metadolomite, metasandstone, metaconglomerate, metasiltstone, quartzite, pelite, phyllite, slate, quartz-mica schist.|
75244|Wartu Monzogranite|66116|5|Briefly described|Map legend|Archean|Archean|Yilgarn Craton. 2643 +/- 6 Ma. Monzogranite; includes minor granite and granodiorite.||||||
75244|Wartu Monzogranite|66117|5|Briefly described|Map legend|Archean|Archean|Yilgarn Craton. c.2643 Ma. Monzogranite; includes minor granite and granodiorite.||||||
75244|Wartu Monzogranite|68107|5|Briefly described|p607 Fig.3, p608 Fig. 4, p609 Tb.1.|Neoarchean|Neoarchean|Mount Venn Greenstone Belt, Burtville Terrane. Post-tectonic. Contains xenocrystic zircons as old as 2932 Ma.|2643 +/- 6 Ma (Wingate et al. 2009).|||Intrudes Palkapiti Formation.|Granite.|
75244|Wartu Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton. Magmatic crystallization age Pb/Pb SHRIMP. See geochron file 179449.1.pdf (2009).|2643+/-6 Ma||||Monzogranite; includes minor granite and granodiorite.|07-AUG-15
75244|Wartu Monzogranite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|See also 100k_geologyp14_lut.csv and 500k_interpgeop14_lut.csv. Age derived from sample of biotite monzogranite (179449.1.pdf).|2643 +/- 6 Ma (SHRIMP).||||Monzogranite; includes minor granite and granodiorite.|
75244|Wartu Monzogranite|70802|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism.|2643+\-6 Ma||||Monzogranite; includes minor granite and granodiorite|
75244|Wartu Monzogranite|71168|6|Mentioned|p10|Neoarchean|Neoarchean|Burtville Terrane, Yilgarn Craton.|2643 +/- 6 Ma|||||
75244|Wartu Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). Sample GSWA 179449 (biotite monzogranite) yielded a weighted mean 207Pb/206Pb date of 2643+\-6 Ma, interpreted to be crystallisation age of the monzogranite. See 100k_interpgeop_lut.csv, 100k_geologyp14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 2_5m_interpgeop15_lut.csv, 100k_geologyl14_lut.csv.|2643+\-6 Ma||||Monzogranite; includes minor granite and granodiorite|
75244|Wartu Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||2643+/-6 Ma||||Monzogranite; includes minor granite and granodiorite.|
24081|Watch Point Formation|22589|6|Mentioned|p125||Proterozoic|||||||
24081|Watch Point Formation|22816|5|Briefly described|p8 Table 1|||Savory Group.||||||30-SEP-08
24081|Watch Point Formation|22901|6|Mentioned|76 fig 2|||Geol Province Officer Basin||||||
24081|Watch Point Formation|22907|6|Mentioned|42|||Geol province Officer Basin. Parent Sunbeam Group||||||
24081|Watch Point Formation|23557|5|Briefly described|p95 Fig.1|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||
24081|Watch Point Formation|24535|5|Briefly described|p4 Fig.2|Neoproterozoic|Neoproterozoic|Of lower part of Sunbeam Group.||||||
24081|Watch Point Formation|41669|4|Described|p50|||||||||
24081|Watch Point Formation|41768|2|Defined|Table 5|Precambrian||||||||
24081|Watch Point Formation|42708|5|Briefly described|Plate 1|Proterozoic||||||||
24081|Watch Point Formation|43055|4|Described|p29, Table 4|||Of Savory Group.||||||30-SEP-08
24081|Watch Point Formation|43056|5|Briefly described|Map Legend|||of Savory Group||||||
24081|Watch Point Formation|43756|4|Described|p535|||||||||
24081|Watch Point Formation|44111|6|Mentioned|p.58, Fig. 2|||in Savory Basin||||||
24081|Watch Point Formation|50008|5|Briefly described|p46 Fig.3|Neoproterozoic||Of Sunbeam Group. Geological Province: Officer Basin.||||||
24081|Watch Point Formation|61732|5|Briefly described|p4 Fig. 3, p58 Fig. 22|Willouran|Willouran|Of the Sunbeam Group. Geological Province: northwestern Officer Basin.||||||07-FEB-11
24081|Watch Point Formation|62453|3|Fully described|p5 Fig. 3, 12 Fig. 8, 22, 53|Cryogenian|Tonian|Of the Sunbeam Group. Geological Province: Officer Basin. Sandstone, siltstone and shale. Thickness: 400m. Unconformably overlies Manganese Group. Overlain by Coondra Formation.||||||
24081|Watch Point Formation|62987|5|Briefly described|p30|Neoproterozoic|Neoproterozoic|Of the Sunbeam Group. Geological Province: Officer Basin.||||||
24081|Watch Point Formation|64580|4|Described|map legend||Neoproterozoic|Of Sunbeam Group. Fine- to medium-grained sandstone, silty sandstone, and shale.||||||09-DEC-08
24081|Watch Point Formation|64772|5|Briefly described|p15|Neoproterozoic|Neoproterozoic|Of the Sunbeam Group. Geological province: Officer Basin.||||||07-FEB-11
24081|Watch Point Formation|64793|6|Mentioned|p283 fig 2|Cryogenian|Cryogenian|Of NW Officer Basin.||||||
24081|Watch Point Formation|65363|6|Mentioned|p5 Fig.4. |Neoproterozoic|Neoproterozoic|||||||
24081|Watch Point Formation|65365|5|Briefly described|p10 Fig. 4|Cryogenian|Cryogenian|Northwestern Officer Basin||||||
24081|Watch Point Formation|65366|5|Briefly described|p23 Fig. 3|Cryogenian|Cryogenian|Northwestern Officer Basin||||||
24081|Watch Point Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|NW Officer Basin.||||||
24081|Watch Point Formation|69185|4|Described|500k_geologyp08_lut.csv||Neoproterozoic|Of Officer Basin.||Unit of Sunbeam Group.|||Fine- to medium-grained sandstone, silty sandstone, and shale|
24081|Watch Point Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||shale, sandstone, siltstone|
24081|Watch Point Formation|72034|5|Briefly described|500k_interpgeop16_lut|Tonian|Tonian|Blake Sub-basin, Officer Basin (Phase 1).||Sunbeam Group|||Fine- to medium-grained sandstone, silty sandstone, and shale.|
31876|Waters Formation|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|Gibson Sub-Basin||||||
31876|Waters Formation|22907|5|Briefly described|41|||||||||
31876|Waters Formation|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Of Tarcunyah Group, Officer Basin.||||||
31876|Waters Formation|23590|6|Mentioned|p22 Appendix 2|||||||||
31876|Waters Formation|23602|4|Described|p16|||Of Tarcunyah Group. Underlying unit Gunanya Sandstone. Max. thickness: 100 m.||||||
31876|Waters Formation|23730|6|Mentioned|p12|||||||||
31876|Waters Formation|23760|4|Described|p26|Proterozoic|Proterozoic|Of Tarcunyah Group. Geological Province: Officer Basin.  Ma. thickness: 100 m.||||||
31876|Waters Formation|43848|5|Briefly described|Map Legend||Proterozoic|Tarcunyah Group.||||||
31876|Waters Formation|49895|6|Mentioned|p10|||On RUDALL (Hickman and Bagas, 1998).||||||23-MAY-16
31876|Waters Formation|50008|5|Briefly described|p46 Fig.3||Neoproterozoic|Of Tarcunyah Group. Geological Province: Officer Basin.||||||
31876|Waters Formation|60470|5|Briefly described|p4 Fig. 2|Neoproterozoic|Neoproterozoic|in Officer Basin, of Tarcunyah Group. Stromatolitic carbonate units, red beds, siltstone, shale, and evaporite units||||||
31876|Waters Formation|62453|3|Fully described|p5 Fig. 3, p65|Cryogenian|Cryogenian|Of the Tarcunyah Group. Geological Province: Paterson Orogen. Correlates with Waroongunyah Formation. Conformably overlies: Gunanya Sandstone. Carbonaceous shale, sandstone, carbonate. ||||||
31876|Waters Formation|64580|6|Mentioned|map legend|||Of Tarcunyah Group.||||||15-DEC-08
31876|Waters Formation|64777|5|Briefly described|p3 Fig.4 |Neoproterozoic|Neoproterozoic||||||Stromatolitic carbonate units, red beds, siltstone, shale and evaporite units.|
31876|Waters Formation|64793|6|Mentioned|p291 fig 8|||||Unit in Tarcunyah Group.||||
31876|Waters Formation|64943|5|Briefly described|p30,37|Neoproterozoic|Neoproterozoic|Of Tarcunyah Group.||||||
31876|Waters Formation|65403|5|Briefly described|p13.|||Probable equivalent to Nooloo (and Choorun) Formations of the Tarcunyah Group.||Unit in Tarcunyah Group.||Conformably overlies Gunanya Sandstone.||
31876|Waters Formation|65454|5|Briefly described|p10|Cryogenian|Cryogenian|Of Throssell Range Group and correlated with Broadhurst Formation (Czarnota et al. 2009). Formerly assigned to Tarcunyah Group (Grey et al. 2005).||||||
31876|Waters Formation|65826|6|Mentioned|p7 Fig.4. |Neoproterozoic|Neoproterozoic|Officer Basin.||||||
31876|Waters Formation|67202|5|Briefly described|p64-65, p231|Neoproterozoic|Neoproterozoic|NW Officer Basin. 350m thick.||Tarcunyah Group.||Overlies Gunanya Sandstone. Correlated with Broadhurst Formation.|Carbonaceous shale, sandstone, siltstone, finely laminated carbonate, shaly units locally sulfidic.|
31876|Waters Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|NW Paterson Orogen.||Tarcunyah Group.||||
31876|Waters Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|Neoproterozoic|Neoproterozoic|||Unit of Tarcunyah Group.||||
31876|Waters Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||shale, crystalline dolostone/dolomite, sulphide-rich rock|
74812|Wattagee Formation|64891|5|Briefly described|p37 Fig. 2, p40-41, p48-9 Tb. 1|Archean|Archean|Of the Glen Group. Conformably overlies Ryansville Formation. Age: 2724-2719Ma. Geological province: Murchison Domain. Thick unit of pillowed komatiite basalt; minor rhyolite; weakly metamorphosed.||||||07-FEB-11
74812|Wattagee Formation|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Mapped as eight separate but un-named units.||Unit in Glen Group.|||Ultramafic schist; pyroxene spinifex-textured basalt; komatiitic basalt, locally pillowed; dacite; quartz-sericite schist; light to dark-grey slate, highly fissile. All metamorphosed.|
74812|Wattagee Formation|67129|6|Mentioned|p18 Fig.19, p38|Archean|Archean|Murchison Domain, Youanmi Terrane.||Glen Group|||Komatiitic basalt; lower greenschist facies.|07-SEP-17
74812|Wattagee Formation|68110|5|Briefly described|p674 Fig. 2|Neoarchean|Neoarchean|Murchison Domain.|c. 2724-2719 Ma|Of the Glen Group.|||Komatiitic basalt.|
74812|Wattagee Formation|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane||Glen Group|Includes 9 unnamed units|Overlies Ryansville Formation.|Slate; Quartz-sericite schist from felsic volcanic rock; intermediate volcanic rock; Dacite; Mafic volcanic rocks; Komatiitic basalt;some pillowed; Pyroxene spinifex-textured basalt, local basalt; Ultramafic schist; all metamorphosed or weathered|
74812|Wattagee Formation|68698|5|Briefly described|p4-5|Neoarchean|Neoarchean|||Glen Group.||Conformably overlies Ryansville Formation.|Komatiitic basalt and subordinate rhyolite.|
74812|Wattagee Formation|69583|4|Described|p47, p49; Plate 2|Neoarchean|Neoarchean|Murchison Domain. On p126, "units of the Wattagee Formation are interpreted to underlie [sic] the Ryansville Formation". The two units are also shown in this order in Plate 2 ; the four Lithology facies are mapped separately.||Glen Group.||Conformably overlies Ryansville Formation.|Fine-grained ultramafic schist derived from komatiitic basalt; ultramafic schist; metamorphosed felsic volcanic rock including andesite, dacite and rhyolite; metamorphosed mafic volcanic rocks.|
74812|Wattagee Formation|69584|5|Briefly described|p5 Fig.2|Neoarchean|Neoarchean|||Glen Group||Overlies the Ryansville Formation|Tholeiitic basalt, felsic volcaniclastic and volcanic rocks.|
74812|Wattagee Formation|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Glen Group.||||
74812|Wattagee Formation|70020|4|Described|p117-118|Neoarchean|Neoarchean|Geological province: Yilgarn Craton. Deposition is coeval with emplacement of Yalgowra Suite within Greensleeves Formation.||Unit of Glen Group.||Underlain by Ryansville Formation.|Komatiitic basalt and subordinate rhyolite.|
74812|Wattagee Formation|70030|5|Briefly described|p192|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton.||Unit of Glen Group.||Upper unit of Glen Group. Underlain by Ryansville Formation.||
74812|Wattagee Formation|70139|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|2735-2700 Ma.|Glen Group.|||Mafic volcanic rock; massive to weakly foliated; locally pillowed and/or vesicular; weakly metamorphosed.|
74812|Wattagee Formation|70418|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|2735-2700 Ma.|Glen Group.|||Ultramafic schist, commonly deeply weathered.|
74812|Wattagee Formation|70796|5|Briefly described|100k_geologyl_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv,  500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 197420.1.pdf, Cue100_2443_stratig.pdf, Madoonga100_2444_stratig.pdf, MountMagnet100_2441_stratig.pdf, Reedy100_2543_stratig.pdf. Numerous additional lithologies are discussed. Misspelt as the Watagee Formation in Madoonga100_2444_stratig.pdf.|ca 7235 Ma2700 Ma (inferred)|Glen Group|||Light to dark grey slate; yellow weathering; highly fissile; metamorphosed. Quartzsericite schist, intermediate volcanic rock, weakly metamorphosed dacite, mafic volcanic rock, komatiitic basalt, pillowed basalt, pyroxenespinifex basalt.|
74812|Wattagee Formation|70830|5|Briefly described|p5, p7, p9|||||Glen Group||Conformably overlies the Ryansville Formation.|Komatiitic basalt and subordinate rhyolite.|
74812|Wattagee Formation|71148|6|Mentioned|p121|||Youanmi terrane.|||||Komatiitic magmatism.|
74812|Wattagee Formation|71168|4|Described|p7-p8|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Coeval with the emplacement of the Yalgowra Suite.|c. 2730-2700 Ma|Glen Group||Overlies the Ryansville Formation.|Komatiitic basalt with subordinate rhyolite.|
74812|Wattagee Formation|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeol_lut.csv.|2735-2700 Ma|Unit of Glen Group.||Underlain by Ryansville Formation.|Slate; weathered, fissile, metamorphosed; quartz-sericite schist and ultramafic schist, deeply weathered; dacite, mafic and felsic volcanics; basalt: komatiitic, pillowed, pyroxene spinifex-textured, weakly metamorphosed.|
74812|Wattagee Formation|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.||Glen Group.|||Ultramafic schist, commonly deeply weathered; quartz-sericite schist derived from felsic volcanic rock, metamorphosed.|
74812|Wattagee Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Youanmi Terrane. 4 unnamed members described.|||||Ultramafic schist from komatiitic basalt. Ultramafic schist; mostly deeply weathered. Felsic volcanics, incl. andesite, dacite, rhyolite; weakly metamorph. Mafic volcanics; massive/weakly foliated; some pillowed +/or vesicular; weakly metamorph.|
74812|Wattagee Formation|73596|5|Briefly described|p1165, 1170|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane.|2725 +/- 4 Ma (Van Kranendonk et al., 2013).|Glen Group.||Coeval with Yalgowra Suite.|Komatiitic basalts, pyroxene spinifex-textured basalts, and subordinate rhyolite.|
24086|Wattle Creek Basalt|42533|3|Fully described|p79|||Name reserved.||||||
24086|Wattle Creek Basalt|44149|5|Briefly described|p33 fig 2-29, p35 fig 2-30, p40,p42,p47|Archean|Archean|See also p57 Fig.2-71. Of Murchison Province. 2km thick. Remnants of a shield volcano.||Mount Farmer Group|||Sequence of massive tholeiite; minor pillow lavas and pyroclastic rocks; silicified and epidotized. Intruded by monzogranite, with abundant microgranite and pegmatite veins near contact.|
24086|Wattle Creek Basalt|65268|6|Mentioned|p6 fig 4, p5 fig 3|||||Unit in Mount Farmer Group.||||
24086|Wattle Creek Basalt|69267|6|Mentioned|p654|||Murchison Province, Yilgarn Craton.||Mount Farmer Group.||||
29720|Weebo Granodiorite|7471|5|Briefly described|p7, Map legend|Archean|Archean|Southern part of the Yandal belt.|||||Hornblende granodiorite.|
29720|Weebo Granodiorite|23281|6|Mentioned|p7|||||||||
29720|Weebo Granodiorite|23591|5|Briefly described|p17|Archean|Archean|2658+/-7 Ma (SHRIMP U-Pb zircon). Geological Province: Yilgarn Craton.||||||07-NOV-08
29720|Weebo Granodiorite|23611|5|Briefly described|p18|||Geological Province: Yilgarn Craton.||||||
29720|Weebo Granodiorite|23930|5|Briefly described|p131|Archean|Archean|Geological Province: Yilgarn Craton. Age: 2666+/-6Ma.||||||07-NOV-08
29720|Weebo Granodiorite|24135|6|Mentioned|p7 Fig. 3|||||||||
29720|Weebo Granodiorite|43289|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
29720|Weebo Granodiorite|60981|5|Briefly described|p175 Fig.1|Archean|Archean|Age: 2658 +/- 7 Ma. Geological Province: Yilgarn Craton.||||||07-NOV-08
29720|Weebo Granodiorite|64586|5|Briefly described|Map legend|Archean|Archean|Granodiorite, both fine- and coarse-grained phases.||||||23-DEC-09
29720|Weebo Granodiorite|65264|5|Briefly described|p48 Appdx. 1|Archean|Archean|Fine-grained granodiorite.||||||07-FEB-11
29720|Weebo Granodiorite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||Includes unnamed fine-grained subunit.||Very coarse grained granodiorite; fine-grained granodiorite.|07-AUG-15
29720|Weebo Granodiorite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Very coarse grained granodiorite.|
29720|Weebo Granodiorite|71270|4|Described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton.|||||Fine- to very coarse-grained granodiorite.|
24088|Weedong Sandstone|40837|6|Mentioned|p261|||||||||
24088|Weedong Sandstone|41169|6|Mentioned|p141|||||||||
24088|Weedong Sandstone|41215|6|Mentioned|p269|||See also Fig.4||||||
70699|Weedy Basalt|62453|5|Briefly described|p5 Fig. 3|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||
69680|Weelumurra beds|61155|5|Briefly described|p16|Middle Miocene|Middle Miocene|Overlies the Kankiangi Clay [?]. Age: ~16.5-14Ma. Thickness: 34m. Geological Province: West Fortescue Valley.||||||07-APR-16
78850|Weerianna Basalt|70775|2|Defined|p12, p22-p23, p94|Paleoarchean|Paleoarchean|East Pilbara. This is a new name defined in Appendix 2 of this report. The type area is located immediately west of Roebourne at Weerianna Hill (from which the name is derived). Up to 1000m thick and outcrops over an area of 100 km ^2 from Mount Wangee, through Roebourne, southwest to Nickol River. Distinguished from the Ruth Well Formation by its lack of peridotitic komatiite and thin chert units. Metamorphosed between greenschist and lower amphibolite facies.|c. 3270 Ma (Minimum age)-3330 Ma (Maximum age)|Roebourne Group||Conformably overlies the Ruth Well Formation. Unconformably overlain by the Nickol River and Dixon Island Formations. Intruded by the Andover Intrusion and the Orpheus Supersuite.|Metamorphosed basalt, including fine-grained komatiitic basalt.|
31771|Weiragoo Granite|23569|4|Described|p6 Tb. 1|Archean|Archean|Of the Murchison Granite-Greenstone Terrane.   Porphyritic to equigranular amphibolite-facies monzogranite.||||||07-NOV-08
31771|Weiragoo Granite|23574|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Meeberrie Gneiss. Underlying unit Cundarra Granite.||||||07-NOV-08
31771|Weiragoo Granite|23576|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Meeberrie Gneiss. Underlying unit Cundarra Granite.||||||07-NOV-08
31771|Weiragoo Granite|23577|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Meeberrie Gneiss. Underlying unit Cundarra Granite.||||||07-NOV-08
31771|Weiragoo Granite|24114|5|Briefly described|p5 Fig.4|Archean|Archean|Geological Province: Yilgarn Craton. Age: c. 2666 Ma.||||||07-NOV-08
31771|Weiragoo Granite|43835|5|Briefly described|Map Legend|Archean|Archean|Age about 2666Ma.||||||07-NOV-08
31771|Weiragoo Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
31771|Weiragoo Granite|71269|6|Mentioned|1m_geologyp12_lut.csv||||||||Heterogeneous, porphyritic to even grained monzogranite with circa 2730 Ma zircon xenocrysts; in places numerous gneissic inclusions. Prograde amphibolite grade metamorphism.|
31771|Weiragoo Granite|73526|5|Briefly described|p2 Fig.1, p3, p12|Neoarchean|Neoarchean|Inferred to comprise a large tract of the NW Youanmi Terrane, SE Narryer Terrane. Comprises at least four dated granitic components, suggests that the age and currently inferred extent is incorrect. See also Weiragoo granite p4 Tb.1, age of 2666+/-6 Ma.|c. 2745 Ma, c. 2690 Ma, c. 2680 Ma, c. 2640 Ma|||||
73395|Welcome Well Formation|65147|5|Briefly described|p4 Fig.3, p5-6, p10, p13-14   |Neoarchean|Neoarchean||2704 +/- 5 Ma (Kositcin et al., in press).|Unit in Minara Group.||Is overlain by Minerie Formation.|Dominated by andesitic conglomerate-sandstone-siltstone facies, intercalated with coherent andesite to basaltic-andesite flows that have pillow structures and associated autoclastic breccia facies.|
73395|Welcome Well Formation|65180|4|Described|map legend|Neoarchean|Neoarchean|Metamorphosed andesite lava and volcaniclastic rocks. Of Minara Group, Murrin Domain, Yilgarn Craton. Age of c.2704 Ma given (after Barley et al., 2002, AMIRA P437A final report p2.18).||||||24-NOV-09
73395|Welcome Well Formation|69152|4|Described|minerie_lut. files||Archean|Murrin Domain,  Kurnalpi Terrane, Yilgarn Craton. GA_OZCHRON U/Pb ages ?from Jul 1994 given for Welcome Well Complex as 2646+/-11 Ma, 2801 +/-10 Ma.|c. 2704 Ma|Minara Group|Includes 13 unnamed subunits.||Basalt; chert/banded chert; jaspilite; felsic volcanic and volcaniclastic rocks; andesite; massive, brecciated; rhyolitic to dacitic siltstone; dacite; rhyolite lava flows, conglomerate, sandstone, and tuff, andesitic; shale; all metamorphosed.|07-AUG-15
73395|Welcome Well Formation|70153|5|Briefly described|Minerie_100k_geologyp_lut.csv|Archean|Archean|See also minerie_100k_interpgeop_lut. csv. |c.2704 Ma.|Minara Group|||Basalt, jaspilite, felsic volcanic and volcaniclastic rocks, massive andesite, brecciated andesite, rhyolitic to dacitic siltstone, dacite, rhyolite, conglomerate with andesitic clasts, sandstone, shale, chert and banded chert.|
73395|Welcome Well Formation|71270|5|Briefly described|GEOL_LUT_CSV files||Archean|Geological province: Murrin Domain, Kurnalpi Terrane, Yilgarn Craton, West Australian Craton. See minerie_100k_geologyp_lut.csv, minerie_100k_geologyl_lut.csv, minerie_100k_interpgeop_lut.csv.||Unit of Minara Group.|||Basalt; andesite: commonly brecciated; chert and banded chert, jaspilite; dacite; felsic volcanics and volcaniclastic sandstone; rhyolite lava flows, rhyolitic to dacitic siltstone, shale. Entire package is weathered and metamorphosed.|
40792|Weld Spring Member|50319|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Glenayle Dolerite. Fine- to medium-grained dolerite with disseminated Fe-Ti oxides; minor sulfides and accessory apatite.||||||28-MAY-04
40792|Weld Spring Member|64655|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Glenayle Dolerite. Fine- to medium-grained dolerite with disseminated Fe-Ti oxides; minor sulfides and accessory apatite; local superposition of sills indicated by l (lower) and u (upper).||||||
40792|Weld Spring Member|64772|5|Briefly described|p13|Mesoproterozoic|Mesoproterozoic|Of the Glenayle Dolerite.||||||07-FEB-11
34479|Weldon Creek Lava member|22754|5|Briefly described|p23|||Informal unit of Koongie Park Formation - see also Weldon Creek lava member and Weldon Creek member.  Max. thickness: >100m.||||||
24092|Wellesley Chert Member|40938|4|Described|p30|||Mention P85||||||
26208|Wells Formation|33800|2|Defined|p138|Archean|Archean|||||||07-NOV-08
26208|Wells Formation|37017|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
26208|Wells Formation|40370|5|Briefly described|p7|||||||||
26208|Wells Formation|40775|4|Described|p494|||||||||
26208|Wells Formation|40785|6|Mentioned|Fig.1|||||||||
26208|Wells Formation|41066|6|Mentioned|2 of 2 C05|||Type area on western flank of Mount Wells. Interdeveloped lavas (andestite, dacite, rhyodacite), tuffs, breccias, agglomerates and minor sediments, all variously deformed and metamorphosed. Maximum thickness ~5.5 km.||||Conformably overlies Hotham Formation, appears to be conformably overlian by Marradong Formation.||14-FEB-18
26208|Wells Formation|41378|5|Briefly described|p81|||||||||
26208|Wells Formation|42165|5|Briefly described|p92|||||||||
26208|Wells Formation|64016|6|Mentioned|p12-13, p12 Fog. 4|Archean|Archean|Age: 2670 to 2650Ma (zircon U-Pb). Felsic volcanic rocks.||||||07-NOV-08
27611|Werillup Formation|9173|5|Briefly described|Map legend.|Eocene|Eocene|||Unit in Plantagenet Group.|||Minor sandstone and conglomerate.|
27611|Werillup Formation|22737|4|Described|13-15,17,18|Late Eocene|Late Eocene|Parent Plantagenet Group. Overlying unit Pallinup Siltstone. Max thickness 49 m||||||
27611|Werillup Formation|23727|5|Briefly described|p109 Fig 66|Oligocene|Eocene|||||||
27611|Werillup Formation|23817|4|Described|p429, 430|Late Eocene|Late Eocene|Geological Province: Bremer Basin. Lowermost unit of the Plantagenet Group. Overlying unit: Pallinup Siltstone (conformable). Max. Thickness: 49m. Contains Lignites up to 3m thick.||||||28-JUL-09
27611|Werillup Formation|24094|4|Described|p269, p277|Middle Eocene|Middle Eocene|Of Plantagenet Group. Overlain by Pallinup Siltstone.||||||16-MAR-05
27611|Werillup Formation|24165|5|Briefly described|p49, p51, p59-60|Eocene|Eocene|Wray Bay area, where it is overlain by subeconomic heavy mineral sands. Hosts a substantial lignite deposit near Scaddan, of possible use for on-site power generation, and at Fitzgerald River.||Plantagenet Group.|||Terrestrial sedimentary rocks: sand, carbonaceous sand, and clay. Hosts lignite.|
27611|Werillup Formation|24358|5|Briefly described|p34|||Geological Province: Bremer Basin.||||||28-JUL-09
27611|Werillup Formation|24397|4|Described|p241|Late Eocene|Late Eocene|The lower part of this unit has been renamed North Royal Formation. Direct equivalent of Pidinga Fm. in SA. Now includes rocks previously included in upper Werillup Fm., Rollos Bore Fm. and Wollubar Sandstone. Geological Province: Eucla Basin.||||||28-JUL-09
27611|Werillup Formation|24410|5|Briefly described|p78 Fig. 38|Tertiary|Tertiary|In the Walpole - Lake Muir area. See also p79 Fig. 39. ||||||
27611|Werillup Formation|29601|6|Mentioned|p82|||||||||
27611|Werillup Formation|30189|5|Briefly described|p132|||L.Eocene.Refs Cockbain(68). See also P133 for lignite distribution.||||||
27611|Werillup Formation|30961|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
27611|Werillup Formation|32648|6|Mentioned|p32|||Tertiary||||||
27611|Werillup Formation|33445|6|Mentioned|p33|||||||||
27611|Werillup Formation|34102|6|Mentioned|p52|||Upper Eocene||||||
27611|Werillup Formation|34103|6|Mentioned|p92|||Algae||||||
27611|Werillup Formation|34432|6|Mentioned|p42|||||||||
27611|Werillup Formation|36890|3|Fully described|p429|||||||||
27611|Werillup Formation|37065|6|Mentioned|p44|||||||||
27611|Werillup Formation|37134|5|Briefly described|p372|||||||||
27611|Werillup Formation|37341|6|Mentioned|p233|||||||||
27611|Werillup Formation|37596|6|Mentioned|p79|||||||||
27611|Werillup Formation|38214|5|Briefly described|p241|||||||||
27611|Werillup Formation|38578|4|Described|p25|||||||||
27611|Werillup Formation|38933|4|Described|p105|||||||||
27611|Werillup Formation|39167|6|Mentioned|p70|||||||||
27611|Werillup Formation|39794|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
27611|Werillup Formation|39795|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
27611|Werillup Formation|40358|6|Mentioned|p23|||||||||
27611|Werillup Formation|40794|5|Briefly described|p92|||||||||
27611|Werillup Formation|41626|6|Mentioned|p50|||||||||
27611|Werillup Formation|41771|6|Mentioned|p49|||See also Fig.6||||||
27611|Werillup Formation|42424|5|Briefly described|p5|||||||||
27611|Werillup Formation|42817|5|Briefly described|p29|||of Plantagenet Group||||||
27611|Werillup Formation|42959|5|Briefly described|p57|||see also p58 Fig.3||||||
27611|Werillup Formation|43065|5|Briefly described|Fig.5,p92|||||||||
27611|Werillup Formation|43283|5|Briefly described|Map Legend||Tertiary|of Plantagenet Group.||||||
27611|Werillup Formation|43498|5|Briefly described|8||Eocene|||||||
27611|Werillup Formation|44145|6|Mentioned|p551  Table 4-27|Eocene|Eocene|||||Correlated with Hampton Sandstone, Pidinga Formation.||
27611|Werillup Formation|44146|4|Described|p562, Fig.4-200, p563 Table 4-28|Eocene|Eocene|Bremer Basin. Max thickness 49m. Type section location in Werillup 3 bore. Has a rich microflora, and fauna in the Limstone Member indicating a late Middle to late Eocene age. Deposited in fluvial, coastal swamp and local delta environments.||Of Plantagenet Group|Includes Nanarup Limestone Member in upper portion.|Transitionally overlain by Pallinup Siltstone.|Dark grey, siltstone, sandstone, claystone, minor brown coal (lignite, carbonaceous siltstone), limestone.|
27611|Werillup Formation|60120|5|Briefly described|p36|Cenozoic|Cenozoic|Brown coals. Contains a single seam as thick as 12m. Geological Province: Bremer and Eucla Basins.||||||28-JUL-09
27611|Werillup Formation|61155|5|Briefly described|p3, p17|Middle Eocene|Middle Eocene|Of the Plantagenet Group. Lignites included. Age: 51.5-39.5Ma. Thickness: 50m. Geological Province: Bremer Basin and Norseman region.||||||
27611|Werillup Formation|62381|5|Briefly described|p9.|Eocene|Eocene|||Plantagenet Group||Is overlain by Pallinup Siltstone.|Clay, siltstone, sandstone and lignite.|03-JUL-14
27611|Werillup Formation|65414|5|Briefly described|p111.|Eocene|Eocene|||Lower unit in Plantagenet Group.||Is overlain by Pallinup Siltstone.|Basal sandstone with lignite and carbonaceous clay.|
27611|Werillup Formation|68811|5|Briefly described|p99, 100, p102-p104, p129 tbl 16|Eocene|Eocene|See also p156 app 1, p185 tbl 42, p187 tbl 43, p188, p189 tbl 44, p188.||Of Plantagenet Group||Overlain by the Pallinup Siltstone.|Fine to coarse-grained sand, lignite and carbonaceous clay.|16-APR-20
27611|Werillup Formation|71789|2|Defined|p99-100||Late Eocene|Part of Plantagent Group [misspelling of Plantagenet Group]. Type section between 56 and 193 ft in Werillup 3 borehore, 30 chains SW of Albany prison.|||Includes Nanarup Limestone Member.|||28-MAY-19
31786|Wesley Yard Monzogranite|22547|3|Fully described|p18||Orosirian|Of the Sally Downs supersuite.||||||14-NOV-06
31786|Wesley Yard Monzogranite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  Age: c. 1835-1805 Ma.||||||07-NOV-08
31786|Wesley Yard Monzogranite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  In the Bow River batholith.  Age: 1835-1805Ma.||||||07-NOV-08
31786|Wesley Yard Monzogranite|43853|5|Briefly described|Map Legend||Proterozoic|||||||
31786|Wesley Yard Monzogranite|44230|5|Briefly described|Map Legend||Proterozoic|||||||
31786|Wesley Yard Monzogranite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Kevins Dam Suite|||Medium- to coarse-grained, porphyritic biotite monzogranite; minor granodiorite|04-AUG-15
31786|Wesley Yard Monzogranite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Kevins Dam Suite|||Medium- to coarse-grained, porphyritic biotite monzogranite; minor granodiorite.|
31786|Wesley Yard Monzogranite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2.|1827-1808 Ma (Inferred)|Unit of Kevins Dam Suite.|||Medium- to coarse-grained, porphyritic biotite monzogranite; minor granodiorite|
31786|Wesley Yard Monzogranite|70154|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1808-1827 Ma|Kevins Dam Suite|||Medium- to coarse-grained, porphyritic biotite monzogranite; minor granodiorite|
31786|Wesley Yard Monzogranite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1827-1808 Ma (inferred)|Unit of Kevins Dam Suite.|||Medium- to coarse-grained, porphyritic biotite monzogranite; minor granodiorite|
31786|Wesley Yard Monzogranite|72437|5|Briefly described|p108|||Whole rock analyses are provided.||Kevins Dam Suite|||Biotite monzogranite, foliated porphyritic biotite monzogranite, biotite tonalite and porphyritic monzogranite.|
29987|West Angela Member|22689|6|Mentioned|Fig. 1 p138|||Of Wittenoom Formation.||||||
29987|West Angela Member|23126|5|Briefly described|p383 Fig.3|||||||||
29987|West Angela Member|24544|4|Described|p57 Fig.43|Archean|Archean|Of Wittenoom Formation. Overlies Mount Newman Member of Marra Mamba Iron Formation. Overlain by Paraburdoo Member. Shale. Geological Province: Hamersley Basin.||||||07-NOV-08
29987|West Angela Member|24573|6|Mentioned|p688|||Of the Wittenoom Formation||||||
29987|West Angela Member|43063|3|Fully described|p49|||Of Wittenoom Dolomite.||||||07-APR-09
29987|West Angela Member|43064|6|Mentioned|p68|||of Wittenoom Formation||||||
29987|West Angela Member|43290|5|Briefly described|p6||Archean|of Wittenoom Formation.||||||07-NOV-08
29987|West Angela Member|60706|5|Briefly described|p625 Fig.3|||Of the Wittenoom Formation. Geological Province: Hamersley Basin.||||||
29987|West Angela Member|62129|3|Fully described|p9|Archaean|Archaean|Of Wittenoom Formation. Thickness: 100m. Geological Province: Hamersley Basin. Consists of dolomite and dolomitic argillite.||||||07-FEB-11
29987|West Angela Member|63153|6|Mentioned|p1361-1363, p1368, p1373, p1375 |||Displays typical fine-grained turbidity-current sedimentation. Mis-spelt as Angelas on p1363, p1368 and p1375.||Unit in Wittenoom Formation.|||Dolomitic shales and carbonates; includes low-grade (50-60 wt % Fe) iron ore deposits, mainly limonite and goethite, with high alumina and silica from interbedded clay.|
29987|West Angela Member|65683|5|Briefly described|p801 Fig2|||Of Wittenoom Formation, Hamersley Group. Overlies Mount Newman Member of Marra Mamba Iron Formation.||||||08-MAR-12
29987|West Angela Member|67130|5|Briefly described|p3 fig 2|||||Wittenoom Formation||Overlies Mount Newman Member, overlain by Paraburdoo Member|Shale|
29987|West Angela Member|67721|5|Briefly described|p38 Fig.9|Neoarchean|Neoarchean|Approximately 0-40 m thick.|c. 2553 Ma|Of the Wittenoom Formation.||||
29987|West Angela Member|68035|5|Briefly described|p292, Fig 6|Neoarchean|Neoarchean|Hamersley Group, Hamersley Basin.||Of Wittenoom Formation.||Overlies Mount Newman Member, Marra Mamba Iron Formation. Overlain by Paraburdoo Member.|Shale.|
29987|West Angela Member|68280|6|Mentioned|p5|||||Wittenoon Formation|||Shale.|
29987|West Angela Member|69538|5|Briefly described|p517 Fig.3, p528-529, p534, p574-576|||See also p583-585. The carbonate content of this unit is susceptible to leaching; deep valleys subsequently developed which were later filled with detrital iron-rich material.||Unit in Wittenoom Formation.||Overlies Marra Mamba Iron Formation.|Shaly dolomite.|
29987|West Angela Member|71808|4|Described|vi, p2, p11, p21-p22, p53, p57|||Hamersley Province. Composition changes from west to east from unaltered to more altered and changes on the basis of original facies change also. Estimated thicknesses range from 0 to over 80m thick, averaging around 40-50m for the central and eastern province. This unit is poorly exposed with typically only a few metres of highly weathered mineralised shale/chert apparent. See also p59, p62, p85, p87, p117, p127, p150, p216, p233.||Wittenoom Formation|||Dolomite and shaly dolomite, manganiferous shale and chert.|
29987|West Angela Member|72447|6|Mentioned|p240|||||Wittenoom Formation||||
29987|West Angela Member|73022|6|Mentioned|p3 Fig.2|||||Wittenoom Formation||Overlies the Mount Newman Member, underlies the Paraburdoo Member.|Shale, minor Fe-chert and banded iron formation.|
29987|West Angela Member|73290|5|Briefly described|p783-785, 797|||||Wittenoom Formation.|||A lower BIF-rich unit, typically mineralised, overlain by a unit of Mn- and Fe-rich shales which show increasing carbonate content with increasing distance from mineralisation. .|
29987|West Angela Member|73538|6|Mentioned|p4|||||Wittenoom Formation||Underlain by the Mount Newman member of the Marra Mamba Iron Formation. Overlain by Paraburdoo Member.|Mudstone/siltstone.|
29987|West Angela Member|73574|6|Mentioned|p762||||||||Shaly.|
24095|West Creek Formation|23724|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Bangemall Group.||||||08-SEP-08
24095|West Creek Formation|23725|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Bangemall Group.||||||
24095|West Creek Formation|24183|6|Mentioned|p10|||||||||
24095|West Creek Formation|41144|3|Fully described|p810|||||||||
24095|West Creek Formation|64287|5|Briefly described|p33, p34 Fig. 2|||Disconformably overlies the Abra polymetallic mineralisation in the Gap Well Formation. Geological Province: Jillawarra Sub-basin - detailed lithology for this basin included.||||||01-FEB-12
24095|West Creek Formation|66241|4|Described|p1, p2, p6, p11. |||Correlates with the lower Kiangi Creek Formation. The lower part of this unit, with the upper part of the underlying Gap Well Formation, hosts the major Abra Pb-Ag-Cu-Au deposit.||||Overlies Gap Well Formation. Is overlain by Jillawarra Formation.|Lower coarse-grained sandstone and polymictic conglomerate; a thick turbidite unit of alternating sandstone, siltstone and minor conglomerate; a local dolostone and siltstone unit; an upper coarse-grained ferruginous sandstone, minor conglomerate.|
80360|West Hinckley Suite|73437|5|Briefly described|p151|Mesoproterozoic|Mesoproterozoic|||Warakurna Supersuite|||Massive gabbro.|
36945|West River gneiss|23727|6|Mentioned|p16|||Informal.||||||
75996|Western Desert Dyke Suite|69003|5|Briefly described|p5, p32|Neoproterozoic|Neoproterozoic|West Arunta Orogen. Appears as Western Dyke Suite on p5. NW-trending dykes intruding the Warumpi Province.|976 +/- 3 Ma.|||||
75996|Western Desert Dyke Suite|69031|5|Briefly described|p4, p8, p23|Tonian|Tonian|Warumpi Province, Arunta Orogen. Crops out mostly E of Kiwirrkura. Produces NW-trending linear magnetic anomalies. Baddeleyite and zircon ages respectively, by Wyborn et al. (1998).|976 +/- 3 Ma; 972 +/- 8 Ma.||||Mafic dykes.|
26209|Westonia Formation|22769|5|Briefly described|Table1p759||Miocene|||||||
26209|Westonia Formation|41199|2|Defined|p6|Tertiary||Reserved as Westonia||||||
26209|Westonia Formation|50621|5|Briefly described|p157, p159 Fig. 2|Cenozoic|Cenozoic|Contains 11 varieties of zircons in the clayey quartz sandstone unit overlying the granitic saprolite (latter contains only 4 varieties).||||||19-NOV-08
26209|Westonia Formation|65385|6|Mentioned|pS133|Miocene|Eocene|Overlies Yilgarn Craton.||||||08-MAR-12
24096|Westralia Sandstone|14227|5|Briefly described|Enclos. 2|Sakmarian|Sakmarian|Presented as Westralia SS. Overlies Stockton Group; underlies Ewington Coal Measures.||||||07-FEB-11
24096|Westralia Sandstone|22820|6|Mentioned|p16|||Of the Collie Group.||||||11-AUG-08
24096|Westralia Sandstone|23174|5|Briefly described|Fig5p8|||||||||
24096|Westralia Sandstone|42711|2|Defined|p4 Fig. 3, p20, Plates 2, 4|Early Permian|Early Permian|Of Collie Group. Conformably overlies Moorhead Formation; underlies Ewington C.M. - predominantly sandstone succession. Geological province: Collie Basin. Detailed lithology given.||||||29-APR-09
24096|Westralia Sandstone|43442|6|Mentioned|p50|||||||||
24096|Westralia Sandstone|64580|5|Briefly described|map legend|||Of Collie Group. Sandstone with interbedded subordinate siltstone in coarsening-upward sequence.||||||15-DEC-08
24096|Westralia Sandstone|64630|5|Briefly described|p31 Fig.2|Artinskian|Sakmarian|Province: Collie Subbasin. Overlies the Stockton Group, underlies the Ewington Coal Measures. Palynology age: P. pseudoreticulata to S. fusus. Base correlates with the base of the Woodynook Sandstone.||||||24-NOV-09
24096|Westralia Sandstone|70097|5|Briefly described|p19 Fig.3|Sakmarian|Sakmarian|Southern Perth Basin. Collie Sub-basin.||Collie Group||Overlies Moorhead Formation. Is overlain by Ewington Coal Measures.|Sandstone.|12-SEP-17
24096|Westralia Sandstone|70774|5|Briefly described|p5 fig 3|Artinskian|Sakmarian|Collie Basin.||||Overlies the Moorehead Formation (Stockton Group). Overlain by the Ewington Coal Measrues.||
24096|Westralia Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Sakmarian|Sakmarian|Perth Basin.  Age from biostratigraphy.||Collie Group.|||Sandstone with interbedded subordinate siltstone in coarsening-upward sequence.|
27096|Whaleback Shale Member|23046|6|Mentioned|171|||||||||
27096|Whaleback Shale Member|23126|5|Briefly described|p383 Fig.3|||||||||
27096|Whaleback Shale Member|23194|6|Mentioned|p42|||Hamersley Province||||||
27096|Whaleback Shale Member|23536|5|Briefly described|Fig 2 p 429|||||||||
27096|Whaleback Shale Member|23612|5|Briefly described|p843|||Of Brockman Iron Formation||||||
27096|Whaleback Shale Member|24041|5|Briefly described|p492|Paleoproterozoic|Archean|Of the Brockman Iron Formation.||||||07-NOV-08
27096|Whaleback Shale Member|24231|5|Briefly described|p186 Fig.2|||Of Brockman Iron Formation. Geological Province: Hamersley Basin.||||||
27096|Whaleback Shale Member|24426|4|Described|p221|Paleoproterozoic|Archean|Of Brockman Iron Formation. Thickness: ~65 m. black shale, chert and carbonates. Overlies Dales Gorge Member. Overlain by Joffre Member. Geological Province: Hamersley Province.||||||07-FEB-11
27096|Whaleback Shale Member|24544|4|Described|p57 Fig.43|Paleoproterozoic|Paleoproterozoic|Of Brockman Iron Formation. Overlies Dales Gorge Member. Overlain by Joffre Member. Age: 2463 Ma. Geological Province: Hamersley Basin.||||||07-NOV-08
27096|Whaleback Shale Member|29596|6|Mentioned|Fig.2|||||||||
27096|Whaleback Shale Member|29629|5|Briefly described|p899|||||||||
27096|Whaleback Shale Member|29716|4|Described|Table 1|||||||||
27096|Whaleback Shale Member|31021|5|Briefly described|p893|||||||||
27096|Whaleback Shale Member|31670|4|Described|p913|||||||||
27096|Whaleback Shale Member|31671|5|Briefly described|p11|||||||||
27096|Whaleback Shale Member|32326|6|Mentioned|p122|||Hamersley Gp.||||||
27096|Whaleback Shale Member|33542|6|Mentioned|p412|||||||||
27096|Whaleback Shale Member|33544|1|Redefined|p73|Precambrian|Precambrian|See also p74.||||||07-JAN-08
27096|Whaleback Shale Member|33545|5|Briefly described|p113|||||||||
27096|Whaleback Shale Member|33687|5|Briefly described|p917|||Also p920 re. mineralization.||||||07-JAN-08
27096|Whaleback Shale Member|34541|6|Mentioned|p53|||See also p54, Plate 25.||||||07-JAN-08
27096|Whaleback Shale Member|34542|6|Mentioned|p94|||||||||
27096|Whaleback Shale Member|35052|6|Mentioned|Fig.2|||||||||
27096|Whaleback Shale Member|35260|6|Mentioned|Fig.4|||||||||
27096|Whaleback Shale Member|35299|5|Briefly described|p893|||||||||
27096|Whaleback Shale Member|36091|5|Briefly described|p572|||||||||
27096|Whaleback Shale Member|36247|6|Mentioned|Fig.2|||||||||
27096|Whaleback Shale Member|36260|5|Briefly described|p78|Paleoproterozoic|Paleoproterozoic|Of the Brockman Iron Formation. Geological Province: Hamersley Basin.||||||07-NOV-08
27096|Whaleback Shale Member|36642|6|Mentioned|Table 1|||||||||
27096|Whaleback Shale Member|36882|4|Described|p134|||||||||
27096|Whaleback Shale Member|37297|6|Mentioned|Fig.2|||||||||
27096|Whaleback Shale Member|37460|6|Mentioned|Fig.3.4|||||||||
27096|Whaleback Shale Member|37577|6|Mentioned|p30|||||||||
27096|Whaleback Shale Member|37704|6|Mentioned|Fig.1|||||||||
27096|Whaleback Shale Member|37708|6|Mentioned|p1930|||||||||
27096|Whaleback Shale Member|38790|6|Mentioned|p164|||||||||
27096|Whaleback Shale Member|39200|6|Mentioned|p286|||||||||
27096|Whaleback Shale Member|39697|6|Mentioned|p126|||||||||
27096|Whaleback Shale Member|41358|5|Briefly described|p146|||||||||
27096|Whaleback Shale Member|41768|5|Briefly described|p28|||||||||
27096|Whaleback Shale Member|42112|5|Briefly described|p9|||See also Table 1||||||
27096|Whaleback Shale Member|42190|6|Mentioned|p280|||||||||
27096|Whaleback Shale Member|42471|4|Described|p8|||Of Brockman Iron Formation.||||||07-JAN-08
27096|Whaleback Shale Member|42495|6|Mentioned|p2, p35|||||||||
27096|Whaleback Shale Member|42686|5|Briefly described|map legend|Proterozoic|Archean|||||||07-NOV-08
27096|Whaleback Shale Member|42744|4|Described|p5|||Of Brockman Iron Formation.||||||07-JAN-08
27096|Whaleback Shale Member|43119|5|Briefly described|p10|||Of Brockman Iron Formation.||||||07-JAN-08
27096|Whaleback Shale Member|43210|5|Briefly described|Table 1 p3,p5.||Mesoproterozoic|Of Brockman Iron Formation.||||||07-JAN-08
27096|Whaleback Shale Member|43262|5|Briefly described|Map Legend||Proterozoic|Of Brockman Iron Formation.||||||07-JAN-08
27096|Whaleback Shale Member|43290|5|Briefly described|p6||Proterozoic|Of Brockman Iron Formation.||||||07-JAN-08
27096|Whaleback Shale Member|43595|6|Mentioned|Fig.2-49,p220|||||||||
27096|Whaleback Shale Member|44152|5|Briefly described|p178-179, p186-187|||Chemical composition on page 187. The "shale" may not be terrigenous clay or mud; rather a variant iron-formation.||Brockman Iron Formation||Overlies Dales Gorge Member. Is overlain by Joffre Member.|Shale.|
27096|Whaleback Shale Member|50227|5|Briefly described|p442|||Of Brockman Iron Fm. Contains a unit called Central Chert (informal name) - very podiform layers of near-pure chert. Overlain by the Joffre Member; underlain by Dales Gorge Member. Max. thickness: ~60m. Geol Prov: Hamersley Prov.||||||07-FEB-11
27096|Whaleback Shale Member|60373|6|Mentioned|p145 Tb. 1|Archean|Archean|Of Brockman Iron Formation.||||||23-JUN-09
27096|Whaleback Shale Member|60706|5|Briefly described|p623 Fig.2, p631|Paleoproterozoic|Paleoproterozoic|Of the Brockman Iron Formation. Thin band of iron formation rocks with significant sheet-silicate content causing a shaly appearance. Age: 2463+/-5 Ma (SHRIMP). Geological Province: Hamersley Basin. See also Appendix 1 p643.||||||07-NOV-08
27096|Whaleback Shale Member|62129|3|Fully described|p10|Archaean|Archaean|Of Brockman Iron Formation. Overlies Dales George Member. Thickness: 75m. Geological Province: Hamersley Basin. Consists of interlayered chert and shale with two BIF bands near the base.||||||27-MAR-13
27096|Whaleback Shale Member|63153|6|Mentioned|p1360, p1362 Fig.3. |||Shows tighter, almost convoluted, folding.||Unit in Brockman Iron Formation.||||
27096|Whaleback Shale Member|64406|5|Briefly described|p1-2|||Of the Brockman Iron Formation. Overlain by Joffre Member. Geological Province: Hamersley Basin.  Discussed in the context of its use as facing stone forming the lift panels in Mineral House, Perth.||||||29-SEP-08
27096|Whaleback Shale Member|64725|6|Mentioned|p58.|||||Unit in Brockman Iron-formation.||Overlies Dales Gorge Member.Is overlain by Joffre Member.||
27096|Whaleback Shale Member|65683|5|Briefly described|p801 Fig2|||Of Brockman Iron Formation. Underlies Joffre Member; overlies Dales Gorge Member.||||||08-MAR-12
27096|Whaleback Shale Member|67025|5|Briefly described|p319.|||||Unit in Brockman Iron Formation.||Conformably overlies Dales Gorge Member. Is overlain conformably by Joffre Member.||
27096|Whaleback Shale Member|67130|5|Briefly described|p3 fig 2|||||Brockman Iron Formation||Overlies Dales Gorge Member, overlain by Joffre Member|Shale.|
27096|Whaleback Shale Member|67201|4|Described|p34 Fig.18, p52, p54, p56|||Shown as Whaleback Shale Mbr. Also abbreviated once as Whaleback Shale. A recessive unit.|c. 2463 Ma, U-Pb SHRIMP|Brockman Iron Formation||Overlies Dales Gorge Member, and is overlain by Joffre Member.||25-NOV-16
27096|Whaleback Shale Member|67721|5|Briefly described|p38 Fig.9|Siderian|Siderian|Approximately 50 m thick.|c. 2463 Ma|Of the Brockman iron formation.||||
27096|Whaleback Shale Member|68035|4|Described|p292 Fig 6|Paleoproterozoic|Paleoproterozoic|Hamersley Group, Hamersley Basin.|2463+/-5 Ma|Of Brockman Iron Formation.||Overlies Dales Gorge Member. Overlain by Joffre Member.|Shale.|
27096|Whaleback Shale Member|68280|5|Briefly described|p5, p41|||||Brockman Iron Formation||Overlain by Joffre Member, overlies Dales Gorge Member|Shale.|
27096|Whaleback Shale Member|69538|5|Briefly described|p517 Fig.3, p529 Fig.9, p531 Fig.11|||See also p564 Fig.37, p568, p583-585. Appears in Figs.3 and 6 as Mt Whaleback Shale, and as Mt Whaleback Shale Member on p525, 531 and 564, 568.||Unit in Brockman Iron Formation.||Overlies Dales Gorge Member. Is overlain by Joffre Member.||
27096|Whaleback Shale Member|69563|6|Mentioned|p691 Fig.1|||||Unit in Brockman Iron Formation.||||
27096|Whaleback Shale Member|69745|6|Mentioned|p277-279, 281-282, 284, 288-290|||Mount Wall area, Hamersley Province.||Brockman Iron Formation.|||Chert, shale. Highly ferruginised close to iron ores.|
27096|Whaleback Shale Member|70509|5|Briefly described|p14|Paleoproterozoic|Paleoproterozoic|Geological province: Hamersley Province; Pilbara Craton. Underwent minor folding and basinal uplift; associated low-grade regional metamorphism from burial prehnite-pumpellyite facies to greenschist facies (Smith et al., 1982).||Unit of Brockman Iron Formation.||Overlain by Joffre Member. Underlain by Dales Gorge Member.||
27096|Whaleback Shale Member|71513|6|Mentioned|P67|||Intersected in drillholes DDH44 and Mitchell-2.||Brockman Iron Formation||||
27096|Whaleback Shale Member|71785|6|Mentioned|p87, 89|||Member Brockman Iron Fm.  Ref to Ryan and Blockley, 1965.||||||
27096|Whaleback Shale Member|72493|5|Briefly described|p29-30|||Hamersley Basin.||Brockman Iron Formation.||Overlies Dales Gorge Member. Is overlain by Joffre Member.|Shale.|
27096|Whaleback Shale Member|72712|6|Mentioned|p10.|Siderian|Siderian|Easily recognizable despite the tight folding in the core of the Hardey Syncline.|c. 2495 Ma to c. 2460 Ma.|Brockman Iron Formation||Probably overlies Dales Gorge Member. Probably overlain by Joffre Member.|Includes shales.|
27096|Whaleback Shale Member|72758|5|Briefly described|p15 Tb.1, p25.|||Occurances of this unit are present over much of north eastern Wyloo.||Brockman Iron Formation|||Includes banded iron formation and mudstone and black, laminated mudstone and contain subordinate chert and carbonate.|
27096|Whaleback Shale Member|73022|6|Mentioned|p2 Fig.1, p3 Fig.2|||||Brockman Iron Formation||Overlies the Dales Gorge Member, underlies the Joffre Member.|Shale, minor Fe-chert and banded iron formation.|
27096|Whaleback Shale Member|73290|6|Mentioned|p784|||Hamersley Province.||||||
83639|Whaling Cove basaltic sill|73480|5|Briefly described|p210-211||Stenian|Maximum crystallisation LA-ICPMS U-Pb zircon age 1444+/-7 Ma. Plagioclase analyses from WC1 yielded a disturbed, stairstepping 40Ar/39Ar spectrum. Dates range from 550 Ma at low-temperature extraction to 800 Ma at high-temperature extraction. Maximum age of ca 1190-1170 Ma constrained from Burnside Batholith migmatitic gneiss host rock, which is part of the Esperance Supersuite. See also Whaling Cove intrusion p216, Whaling Cove sill p217. This sub-horizontal and  N-NW trending sill also cuts older E-NE trending dykes.|||||Porphyritic ophitic basalt, metamorphosed.|
80104|Wheatbelt Dyke Suite|70826|6|Mentioned|p14 tbl 5|Ectasian|Ectasian|West Yilgarn Craton.|1215-1205 Ma|||||
26211|Whim Creek Group|22449|6|Mentioned|Fig27 P26||Archean|Age of unit is 3010 Ma||||||07-NOV-08
26211|Whim Creek Group|22715|5|Briefly described|table7, p214,216|Archean|Archean|||||||07-NOV-08
26211|Whim Creek Group|22727|6|Mentioned|p635||Archean|||||||07-NOV-08
26211|Whim Creek Group|23046|6|Mentioned|167|||Geol province Pilbara Craton. Overlying unit Louden Volcanics||||||
26211|Whim Creek Group|23244|5|Briefly described|p19||Archean|Minimum age determined by Kialrah Rhyolite - 2972 +/-2Ma. of Whim Creek Belt.||||||07-NOV-08
26211|Whim Creek Group|23255|6|Mentioned|p46, 48||Archean|Age: Constrained between 3100 and 2900 Ma. Correlated to the Lalla Rookh Bain.||||||07-NOV-08
26211|Whim Creek Group|23348|4|Described|217|Archean|Archean|3010-2950Ma||||||07-NOV-08
26211|Whim Creek Group|23484|5|Briefly described|p10 table 3|Archean|Archean|Geological Province: Mallina Basin.||||||07-NOV-08
26211|Whim Creek Group|23598|6|Mentioned|p3|Archean|Archean|Of Pilbara Supergroup. Overlying unit Louden Volcanics. Geological Province: Pilbara Craton.||||||07-NOV-08
26211|Whim Creek Group|23743|4|Described|p4|Archean|Archean|Age: c.3000 Ma. Of Pilbara Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
26211|Whim Creek Group|23755|5|Briefly described|p8|||||||||
26211|Whim Creek Group|23780|5|Briefly described|p164|Archean|Archean|Age: ~3016+/-3 Ma||||||07-NOV-08
26211|Whim Creek Group|23783|5|Briefly described|p3|||||||||
26211|Whim Creek Group|23784|5|Briefly described|p20|Archean|Archean|||||||07-NOV-08
26211|Whim Creek Group|23789|4|Described|p21|Archean|Archean|Age: c.3010Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
26211|Whim Creek Group|23793|4|Described|p19|Archean|Archean|Age: c.3010Ma  Of Pilbara Supergroup||||||07-NOV-08
26211|Whim Creek Group|23794|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup. Geological Province Pilbara Craton.||||||07-NOV-08
26211|Whim Creek Group|23813|5|Briefly described|p98|Archean|Archean|Amygdaloidal basalt, basaltic tuff and epiclastic sandstone, flow-banded rhyolite and rhyodacite.  Age: 3010Ma. Geological Province: Pilbara Craton.  See also p90 Tb. 1.||||||07-NOV-08
26211|Whim Creek Group|23936|5|Briefly described|p3, p6, Tb.1, Fig.4|Archean|Archean|Age: ca. 3015-2950 Ma. Geological Province: Pilbara Craton. Correlates directly with Mallina Formation and Constantine Sandstone.||||||07-NOV-08
26211|Whim Creek Group|24023|4|Described|p18|Archean|Archean|Of the Pilbara Supergroup.||||||07-NOV-08
26211|Whim Creek Group|24024|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
26211|Whim Creek Group|24025|4|Described|p8 Tb. 1|Archean|Archean|Felsic volcanic and sedimentary rocks (interpreted from aeromagnetic data).  Age: c.3009Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
26211|Whim Creek Group|24095|4|Described|p46|||Uppermost unit of the Pilbara Supergroup.  Overlies the Gorge Creek Group. Geological Province: Pilbara Block.||||||30-MAR-05
26211|Whim Creek Group|24110|5|Briefly described|Plate 1|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
26211|Whim Creek Group|24140|3|Fully described|p215-216, p214 Fig. 1|Archean|Archean|Originally comprised Warambie Basalt, Mons Cupri Volcanics, Constantine Sandstone and Mallina Formation (Fitton et al 1975); then Rushall Slate, Cistern Formation, Mons Cupri Volcanics (SmOverlain by Bookingarra Group.  Geological Province: Mallina Basin||||||14-OCT-15
26211|Whim Creek Group|24166|5|Briefly described|p3|Archean|Archean|Parent: Pilbara Supergroup||||||07-NOV-08
26211|Whim Creek Group|24169|5|Briefly described|p666 Fig. 5|||||||||
26211|Whim Creek Group|24184|4|Described|p709, 714, 715|Archean|Archean|Geological Province: Mallina Basin. Age: 3016 +/- 3 -- 3009 +/- 4Ma (Nelson 1998, 2002). Two units, Cistern Formation and Rushall Slate (Hickman 1983) now reassigned to the Bookingarra Group||||||07-NOV-08
26211|Whim Creek Group|24185|5|Briefly described|p735 Fig. 2|Archean|Archean|Age: 3.02-2.95 Ga. Geological Province: Mallina Basin.||||||07-NOV-08
26211|Whim Creek Group|24189|5|Briefly described|p802 Fig.1|Archean|Archean|Geological Province: Mallina basin||||||07-NOV-08
26211|Whim Creek Group|24190|6|Mentioned|p820 Fig.1|||||||||
26211|Whim Creek Group|24191|4|Described|p828 Fig. 1, p831|Archean|Archean|Parts of original Whim Creek Gp. now included in Bookingarra Group.  Now includes Warambie Basalt, Red Hill Volcanics and Mons Cupri Dacite.  Overlain by Bookingarra Gp. Age: 3009+/-9Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
26211|Whim Creek Group|24192|5|Briefly described|p860|Archean|Archean|Underlying Unit: Bookingarra Group. Geological Province: Pilbara Craton. Age: 3010-2990 Ma (Smithies et al, 1998)||||||07-NOV-08
26211|Whim Creek Group|24193|5|Briefly described|p875 Fig2|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
26211|Whim Creek Group|24353|4|Described|p5, p6 Fig.4|Archean|Archean|Overlying Unit: Louden Volcanics. Underlying Unit: Cleaverville Formation. Age: c.3010Ma. Geological Province: Manilla Basin||||||07-NOV-08
26211|Whim Creek Group|24391|5|Briefly described|p8-2|Archean|Archean|Age: 2991 Ma. Geological Province: Pilbara Block.||||||07-NOV-08
26211|Whim Creek Group|24541|6|Mentioned|p14, p19 Fig.5|||Geological Province: West Pilbara Granite-Greenstone Terrane. Of the Pilbara Supergroup.||||||
26211|Whim Creek Group|24550|5|Briefly described|p36 Tb. 3.2|Archean|Archean|Basalt, rhyolite, sandstone. Unconformably overlies the Whundo Group. Age: 3010Ma. Geological Province: Pilbara Craton. See also p74 Tb. 5.1.||||||07-FEB-11
26211|Whim Creek Group|24590|5|Briefly described|p81 Fig. 3.1|||In the granite-greenstone terrain of the Pilbara.||||||07-FEB-11
26211|Whim Creek Group|30363|6|Mentioned|p10|||||||||
26211|Whim Creek Group|30766|2|Defined|Appendix|Precambrian|Precambrian|||||||
26211|Whim Creek Group|31310|4|Described|p53|||||||||
26211|Whim Creek Group|32954|6|Mentioned|p187|||||||||
26211|Whim Creek Group|34829|4|Described|p67|||||||||
26211|Whim Creek Group|35269|6|Mentioned|p297|||||||||
26211|Whim Creek Group|36257|6|Mentioned|p29|||||||||
26211|Whim Creek Group|36551|6|Mentioned|p25|||See also P55.||||||
26211|Whim Creek Group|37299|6|Mentioned|Fig.1|||||||||
26211|Whim Creek Group|37373|6|Mentioned|p80|||||||||
26211|Whim Creek Group|38113|6|Mentioned|p33|||||||||
26211|Whim Creek Group|38498|6|Mentioned|Fig.1|||||||||
26211|Whim Creek Group|39580|4|Described|p290|||||||||
26211|Whim Creek Group|39672|6|Mentioned|Fig.2|||||||||
26211|Whim Creek Group|39697|3|Fully described|p104|||||||||
26211|Whim Creek Group|39837|6|Mentioned|p258|||||||||
26211|Whim Creek Group|40596|6|Mentioned|Fig.1|||||||||
26211|Whim Creek Group|40815|4|Described|p275|||||||||
26211|Whim Creek Group|41028|5|Briefly described|p227|||||||||
26211|Whim Creek Group|41073|6|Mentioned|p200|||||||||
26211|Whim Creek Group|41250|5|Briefly described|p29|||||||||
26211|Whim Creek Group|41252|6|Mentioned|p50|||||||||
26211|Whim Creek Group|41263|6|Mentioned|p57|||||||||
26211|Whim Creek Group|41349|6|Mentioned|p4|||||||||
26211|Whim Creek Group|41357|6|Mentioned|Fig.1|||||||||
26211|Whim Creek Group|41358|6|Mentioned|Fig.1|||||||||
26211|Whim Creek Group|41635|6|Mentioned|p21|||||||||
26211|Whim Creek Group|41678|5|Briefly described|p31|||||||||
26211|Whim Creek Group|42231|4|Described|p334|||||||||
26211|Whim Creek Group|42260|6|Mentioned|p6|||||||||
26211|Whim Creek Group|42329|5|Briefly described|p5|||||||||
26211|Whim Creek Group|42707|5|Briefly described|map legend|Archean||||||||07-NOV-08
26211|Whim Creek Group|42730|4|Described|p4|||See also Fig 2, P5||||||
26211|Whim Creek Group|42785|6|Mentioned|p270|||||||||
26211|Whim Creek Group|42973|5|Briefly described|p175|||||||||
26211|Whim Creek Group|43052|5|Briefly described|Fig.3.8|||||||||
26211|Whim Creek Group|43595|6|Mentioned|Fig.2-47,211|||||||||
26211|Whim Creek Group|43698|6|Mentioned|p3||Archean|Late Archaean||||||07-NOV-08
26211|Whim Creek Group|43769|6|Mentioned|p855|||Age: 2.99 Ga||||||
26211|Whim Creek Group|43779|6|Mentioned|p5|||||||||
26211|Whim Creek Group|43821|5|Briefly described|map legend|Archean|Archean|Of Pilbara Supergroup.||||||07-NOV-08
26211|Whim Creek Group|44150|4|Described|p129 Tb.2-15, p132 Figs.2-131,-132, p137|||See also p140-142, p152 Tb.2-22, p157 Fig.2-144. 500-1000m thick.|c.3.0 Ga.|Pilbara Supergroup|Warambie Basalt, Mons Cupri Volcanics, Rushall Slate.|Overlain unconformably by Mount Roe Basalt. Overlies Warrawoona Group unconformably; overlies Mosquito Creek Formation disconformably.||
26211|Whim Creek Group|44863|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
26211|Whim Creek Group|46319|5|Briefly described|p4|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
26211|Whim Creek Group|50430|5|Briefly described|p158 Tb.1||Archean|Recently assigned to Whim Creek Basin. Previously in Mallina Basin.||||||07-NOV-08
26211|Whim Creek Group|60362|5|Briefly described|p1516, p1518, p1534|Archean|Archean|Basement to NW Mallina Basin.|c.3.01 Ga.|||Is overlain unconformably by Bookingarra Group.|Felsic volcanic and volcaniclastic rocks.|
26211|Whim Creek Group|60429|6|Mentioned|p18|||||||||07-FEB-11
26211|Whim Creek Group|61253|5|Briefly described|p53, p52 Fig. 2|Archean|Archean|Overlain by Bookingarra Group and De Grey Supergroup.  Age: ~3.02-2.97Ga.  Geological province: Pilbara Craton.  Probably cogenetic with Maitland River Supersuite.  See also p50 Fig. 1, p56, p58.||||||07-NOV-08
26211|Whim Creek Group|63441|5|Briefly described|p5 Tb. 1, p14 Fig. 2, p27|Archean|Archean|Of De Grey Supergroup. Comprises Warambie Basalt and Red Hill Volcanics which overlie and are partly interbedded with the basalt. Age: 3010Ma, 3009+/-4Ma. Geological province: Whim Creek Basin, Pilbara Craton.||||||07-FEB-11
26211|Whim Creek Group|63538|4|Described|p2 Fig. 1, p7, p31, p32|Archean|Archean|Inc; Warambie Basalt. Unconform overlies Whundo Gp and Cleaverville Fm, disconformably overlain by Croydon Group. Age: 3010 Ma. Geological Province: De Grey Superbasin. Coeval felsic to mafic volcanic, intrusive, and volcaniclastic rocks.||||||17-APR-13
26211|Whim Creek Group|64174|5|Briefly described|Map legend|Archean|Archean|Of De Grey Supergroup. Includes Red Hill Volcanics and Warambie Basalt. Age: <3016-3009Ma. Geological province: Whim Creek Basin, Pilbara Craton.||||||07-NOV-08
26211|Whim Creek Group|64580|4|Described|map legend||Mesoarchean|Felsic volcanic and sedimentary rocks; interpreted from aeromagnetic data.||||||09-DEC-08
26211|Whim Creek Group|64632|5|Briefly described|p201 Fig.1, p203, 207|Mesoarchean|Mesoarchean|Unconformably underlain by both the Whundo and Gorge Creek Groups along the western margin of the Mallina Basin.|3010-2980 Ma|Of the De Grey Supergroup.||Unconformably underlain by the the Whundo Group. Unconformably underlain by the Gorge Creek Group.|Comprises a complex association of coeval mafic to felsic volcanic, volcaniclastic, and intrusive rocks.|
26211|Whim Creek Group|65415|4|Described|pp118-123.|Archean|Archean|Has shallow dips away from Caines Well Granite; is preserved as an apron around an unroofed domal fold structure. Upper part hosts significant massive-sulfide mineralisation at Whim Creek and Mons Cupri. May correlate with part of the Mallina Formation.|c.2.99 Ga (Barley et al. 1994).|Unit in Pilbara Supergroup.|Includes Mons Cupri Volcanics, Cistern Formation and Rushall Slate.|Unconformably overlies Caines Well Granite. Is overlain conformably by Louden Volcanics.||
26211|Whim Creek Group|65825|6|Mentioned|p2 Fig.1. |||Central Pilbara Tectonic Zone, North Pilbara Craton.||||||
26211|Whim Creek Group|65827|6|Mentioned|p3 Fig.1|||Central Pilbara Tectonic Zone.||||||21-JAN-22
26211|Whim Creek Group|65829|6|Mentioned|p2 Fig.1. |||Central Pilbara Tectonic Zone.||||||
26211|Whim Creek Group|66118|5|Briefly described|p146 Fig.1, p147, p158 Tb.2|||Pilbara Craton.|3010 Ma|De Grey Supergroup||Is unconformably overlain by Croydon and Nullagine Groups. Unconformably overlies Gorge Creek Group.||
26211|Whim Creek Group|66217|5|Briefly described|p9, pp39-40.|Mesoarchean|Mesoarchean|Whim Creek Basin, SE margin of West Pilbara Superterrane. Deposition is suggested to have followed break-off of the subducted slab associated with formation of the Whundo Group intra-oceanic arc. Hosts volcanigenic Cu-Zn massive sulfide deposits.|3.01 Ga.|Unit in De Grey Supergroup.|Includes Warambie Basalt and Red Hill Volcanics.|||
26211|Whim Creek Group|67130|6|Mentioned|p13, p14 fig 9|Mesoarchean|Mesoarchean||3020 Ma- 2970 Ma|De Grey Supergroup||Overlies Gorge Creek Group, overlain by De Grey Supergroup||
26211|Whim Creek Group|67201|4|Described|p7, p12, p13, p15-17, see comments|Archean|Archean|In northwestern Pilbara Craton, unconformably overlies West Pilbara Superterrane and East Pilbara Terrane. Comprises all of Whim Creek Basin, De Grey Superbasin. Page location continued: p20-24, p27, p44, p49, p57, p60, p64.|3010-2990 Ma|De Grey Supergroup|Red Hill Volcanics, Warambie Basalt|Unconformably overlies Gorge Creek Group, Mount Roe Basalt or where absent, Whundo Group. Is unconformably overlain by Cistern Formation and northwest margin units of Mallina Basin.|Felsic volcaniclastic and siliciclastic sedimentary rocks: intrusive porphyritic dacite and dacitic to rhyolitic lava; vesicular basalt and basaltic andesite; sandstone, conglomerate, siltstone and shale; metamorphosed.|25-NOV-16
26211|Whim Creek Group|68035|5|Briefly described|p290, Fig 5|Mesoarchean|Mesoarchean|Whim Creek Basin, De Grey Superbasin. SE of Sholl Shear Zone. A within-plate extensional setting was interpreted.|3.01 - 3.00 Ga||||Volcanic, intrusive, and volcaniclastic rocks.|
26211|Whim Creek Group|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological province: East Pilbara Granite-Greenstone Terrane and Kurrana Terrane, Pilbara Craton. Of Central Pilbara Tectonic Zone; Of Mallina Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|||Includes Red Hill Volcanics, Warambie Basalt.||Felsic volcanic and sedimentary rocks; interpreted from aeromagnetic data|
26211|Whim Creek Group|69299|5|Briefly described|p6 Tb.1, p7, p8 Fig.5, p9 Tb.2|Archean|Archean|Concealed on COOYA POOYA.||||Overlies Whundo Group constituents with a high-angle regional unconformity, and is overlain unconformably by Bookingarra Group constituents on COOYA POOYA.|Dominantly basaltic.|01-JUL-14
26211|Whim Creek Group|69300|5|Briefly described|map legend|Archean|Archean|Whim Creek Basin (and Mallina Basin?), Whim Creek greenstone belt. Older detrital populations ages, c.3058 Ma, c.2985, c.3020, c.3150, Nelson 2000.|<2985 Ma.|Pilbara Supergroup|Red Hill Volcanics, Warambie Basalt|||03-SEP-14
26211|Whim Creek Group|69301|4|Described|p5 Fig.3, p6 Fig.4, p9 Tb.1, p14-16, p23|||Pilbara Craton. West Pilbara Superterrane. Entire Whim Creek Basin.|3000 Ma Red Hill Volcanics|De Grey Supergroup|Red Hill Volcanics, Warambie Basalt|Is unconformably overlain by Cistern Formation.||
26211|Whim Creek Group|69569|6|Mentioned|p285 Fig.1|||East Pilbara Terrane.||||||
26211|Whim Creek Group|69590|4|Described|500k_geologyp08_lut.csv||Mesoarchean||||Includes Red Hill Volcanics.||Felsic volcanic and sedimentary rocks; interpreted from aeromagnetic data|
26211|Whim Creek Group|70022|6|Mentioned|p114-115|||De Grey Superbasin.|3010-2990 Ma.|De Grey Supergroup.|Warambie Basalt, Red Hill Volcanics.|||
26211|Whim Creek Group|70312|6|Mentioned|p2, 6|Archean|Archean|West Pilbara Block.|2940 +/- 20 Ma (Pb-Pb; Gulson et al., 1983).|||||
26211|Whim Creek Group|70775|5|Briefly described|iii, p10, p12-p13, p15, p18, p36|Mesoarchean|Mesoarchean|Following stratigraphic revision of this group (Pike et al., 2002) VHMS mineralization previously assigned to this group is now interpreted to be within the overlying Bookingarra Group. Felsic volcanic rocks of this group are potential correlatives of the Cattle Well Formation. See also  p38-p39, p41, p43, p44 fig 27, p46, p49-p52, p57, p61-p62, p65, p68, p73, p75, p77, p81, p94-p95, p99-p100.|c. 3015-2990 Ma|De Grey Supergroup|Includes the Warambie Basalt and the Red Hill Volcanics.|Unconformably overlies the Gorge Creek Group and the Cleaverville Formation. Unconformably overlain by the Bookingarra Group. Intruded by the Opaline Well Intrusion.||
26211|Whim Creek Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, basalt, volcaniclastic rock, shale|
26211|Whim Creek Group|72034|6|Mentioned|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Red Hill Volcanics, Warambie Basalt.|||
26211|Whim Creek Group|72251|5|Briefly described|p52,54|Mesoarchean|Mesoarchean|Geological province: West Pilbara Superterrane, Pilbara Craton. Of De Grey Superbasin.|3010-2990 Ma|Unit of De Grey Supergroup.|Includes Red Hill Volcanics and Warambie Basalt.|||
26211|Whim Creek Group|72668|4|Described|p3-4, p8, p12-16, p21-22, p25, p28-p29|||West Pilbara Superterrane. Whim Creek Basin. Occupies an isolated fault-bounded basin. Deposited during extensive block faulting and long lived extension following the collision of the WPS and EP. Interpreted to be deposited as part of a continental arc. Hosts VMS mineralisation in addition to the Croydon Group. Only one reliable age date is available from a vitric welded tuff near the top of the group, which yielded an igneous population with an age of 3009 +/- 4 Ma, and two inherited zircons at c. 3.15 Ma.|c. 3010 -2980 Ma|De Grey Supergroup|Includes the Red Hill Volcanics and the Warambie Basalt.|Unconformably overlies the Whundo Group and the Gorge Creek Group. Disconformably overlain by the Croydon Group.|Coeval mafic to felsic volcanic intrusive  and volcaniclastic rocks.|14-JAN-22
77461|Whimbrel Sandstone Member|67370|6|Mentioned|p313 Fig.2. |Triassic|Triassic|||||||
78699|White Desert Member|69788|3|Fully described|p1023, p1029-1034, p1037|Pleistocene|Pleistocene|New name. Eolianites were deposited up to c.100m a.s.l. during interglacial highstands, under the influence of strong S to SW winds. Outcrops as yellow, well-cemented pinnacles up to 1m high. Type locality in White Desert (northern part of Pinnacles Desert) given. Thickness unknown. Age is of a cross-cutting calcite vein; the Member was probably deposited during MIS 13 (533-478 ka) or earlier.|487 +/- 40 ka (U/Th), Lipar and Webb, 2014.|Basal unit in Tamala Limestone.||Overlies Kockatea Shale. Is overlain by Nambung Member.|Consists of an eolian calcarenite/calcrete-microbialite/paleosol cycle.|
78699|White Desert Member|69840|5|Briefly described|p185, p187, p187 Tb1, p190, p196 Fig.13|Pleistocene|Pleistocene|Dating using U/Th geochronology. Marine Isotope stage 12-13 or earlier. See also p197.|0.48700 +/- 0.04000 Ma|Tamala Limestone||Underlies the Nambung Member. Partially overlies Tamala Limestone.|Generally consist of aeolian calcarenite (aeolianite),overlain by calcrete, microbialite and a palaeosol.|
73572|White Hill Road Limestone Member|63454|4|Described|p75|Pleistocene|Pleistocene|Upper part of Tims Thicket Limestone. Aeolianites; cross-laminated to structureless, fine and medium calcarenite. Type location is same as for parent formation. See also White Hill Member.||||||
77943|White Hope Basalt|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2720 - 2680 Ma (inferred).|Two Sisters Subgroup|||Plagioclase-phyric basalt; massive to pillowed; metamorphosed.|
77943|White Hope Basalt|70326|3|Fully described|p336,338-9,341-2,346,350-1,353-4,360-4|Neoarchean|Neoarchean|Geological province: Agnew region, Ora Banda Domain, Kalgoorlie Terrane, Yilgarn Craton. Subaqueous extrusive,megacrystic, highly fractionated and Al- and Fe-rich basalt. Thickness: 300 m. Occurs in the Mount White Syncline, observed in two drillholes and in the field, absent on the western limb of the Agnew anticline. Major and trace element geochemical analysis on Table 4 p342-346. Intruded by Turret Dolerite. Age from detrital zircons, maximum depositional age, U-Pb SHRIMP (Kositcin et al., 2008),|2692+\-3 Ma (Kositcin et al., 2008).|||Overlain by Turrett Dolerite. Underlain by Redeemer Basalt. Correlable to Victorious Basalt.|Massive megacrystic basalt with alkali feldspar crystals as separate grains or glomerocrysts; submarine sheet flows.|
77943|White Hope Basalt|71212|5|Briefly described|intro p2|||Yilgarn Craton. ||Two Sisters Subgroup||Overlain by the Vivien Gabbro.|Megacrystic basalt.|
77943|White Hope Basalt|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2711-2687 Ma (inferred)|Unit of Two Sisters Subgroup.|||Plagioclase-phyric basalt; metamorphosed|
77943|White Hope Basalt|73151|5|Briefly described|p3, p5, p10, p12-13, p16|Neoarchean|Neoarchean|Yilgarn Craton. Kalgoorlie Terrane, Agnew Greenstone Belt.||Kalgoorlie Group||Overlies Redeemer Basalt, underlies Turret Dolerite, Vivien Formation.|Feldspar porphyritic basalt.|
77943|White Hope Basalt|73596|6|Mentioned|p1152, 1156-1158, 1160, 1162-1163|Neoarchean|Neoarchean|Agnew-Wiluna Greenstone Belt. Deep-water mafic-ultramafic lava fields and feeder intrusions.||Two Sisters Subgroup.||Overlies Redeemer Basalt. Is overlain by Vivien Formation (Mount White Group).||
29137|White Lake Metaconglomerate|31042|6|Mentioned|Fig. 2|||||||||
78964|White Rock Leucogranite|44155|5|Briefly described|p239 Tb.3-3, p248 Tb.3-8|Paleoproterozoic|Paleoproterozoic|East Kimberley.||Lamboo Complex||Intruded by Mabel Downs Granodiorite.|Syenogranite, locally garnetiferous or biotite-rich; recrystallized and multiply deformed.|15-JAN-15
26288|Whitewood Formation|41669|2|Defined|Table 5|Precambrian?||Fully described P41||||||
26288|Whitewood Formation|43055|4|Described|p25, Table 4|||of Mangaese Group||||||
26288|Whitewood Formation|43056|5|Briefly described|Map Legend|||of Manganese Group||||||
26288|Whitewood Formation|44142|5|Briefly described|p315 Tb.4-4, p324|||~250m thick fluviatile, alluvial fan deposits. Only found south of Whitewood Fault.||Uppermost Manganese Subgroup.||Overlies Balfour Formation conformably.|Sandstone, conglomerate.|
26288|Whitewood Formation|66107|5|Briefly described|p4 Fig.1|Mesoproterozoic|Mesoproterozoic|||Of the Manganese Group||Overlies Wobblegun Formation. Is overlain by Stag Arrow Formation.||
26288|Whitewood Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, conglomerate|
31020|Whundo Group|22449|5|Briefly described|P28, Fig27, P27||Archean|Age of unit is 3120 Ma||||||07-NOV-08
31020|Whundo Group|23046|5|Briefly described|175|||Age ca 3125-3112 Ma. Overlying unit Cleaverville Formation||||||
31020|Whundo Group|23244|6|Mentioned|Fig.1,2||Archean|Age: ca.3120 Ma.||||||07-NOV-08
31020|Whundo Group|23348|5|Briefly described|217|Archean|Archean|~3120Ma||||||07-NOV-08
31020|Whundo Group|23455|5|Briefly described|p43|Archean|Archean|||||||07-NOV-08
31020|Whundo Group|23484|4|Described|p10 table 3|Archean|Archean|Of Pilbara Supergroup. Geological Province: Pilbara Craton. Age: 3125-3155Ma.||||||07-NOV-08
31020|Whundo Group|23598|5|Briefly described|p5 Fig 3|||Geological Province: Pilbara Craton.||||||
31020|Whundo Group|23743|4|Described|p7|||Geological Province: Pilbara Craton.||||||
31020|Whundo Group|23783|5|Briefly described|p37 Tb. 1|Archean|Archean|||||||07-NOV-08
31020|Whundo Group|23784|4|Described|p10|Archean|Archean|||||||07-NOV-08
31020|Whundo Group|23789|4|Described|p10|Archean|Archean|Age: 3130-3115Ma.  Max. thickness: 10,000m.  Geological Province: Pilbara Craton.||||||07-NOV-08
31020|Whundo Group|23793|4|Described|p15|Archean|Archean|Age: 3125-3115 Ma.  See also page 11 table 2||||||07-NOV-08
31020|Whundo Group|23794|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
31020|Whundo Group|23807|6|Mentioned|p109 Fig. 1|||Geological Province: Pilbara Craton.||||||
31020|Whundo Group|23813|5|Briefly described|p98|Archean|Archean|Calc-alkaline felsic and mafic volcanics, volcanogenic sediment and chert.  Age: 3125Ma. Geological Province: Pilbara Craton.  See also p91 Tb. 1.||||||07-NOV-08
31020|Whundo Group|23936|4|Described|p2, Tb.1|Archean|Archean|Age: ca. 3120 Ma. Geological Province: Pilbara Craton. Overlain by Cleaverville Formation (unconformably). Underlain by Gorge Creek Group (unconformably).||||||07-NOV-08
31020|Whundo Group|24023|5|Briefly described|p5|Archean|Archean|||||||07-NOV-08
31020|Whundo Group|24024|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
31020|Whundo Group|24140|6|Mentioned|p232 Fig. 7|||||||||
31020|Whundo Group|24166|5|Briefly described|p3|Archean|Archean|Age: c.3125Ma||||||07-NOV-08
31020|Whundo Group|24184|4|Described|p711|Neoarchean|Neoarchean|Geological Province: Pilbara Craton. Max Thickness: 10km. Age: 3130-3115Ma||||||07-NOV-08
31020|Whundo Group|24185|5|Briefly described|p735 Fig.2, p739 Tb.3|Archean|Archean|Age: 3124 +/- 4 (SHRIMP zircon U-PB, Smith 1998). Geological Province: Mallina Basin.||||||07-NOV-08
31020|Whundo Group|24191|5|Briefly described|p828 Fig. 1, p829 Tb. 2|Archean|Archean|Age: ca.3120Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
31020|Whundo Group|24192|5|Briefly described|p850|Archean|Archean|Geological Province: Pilbara Craton. Age: 3130-3115 Ma. Felsic metavolcanic rocks||||||07-NOV-08
31020|Whundo Group|24193|5|Briefly described|p875 Fig.2|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
31020|Whundo Group|24352|5|Briefly described|Map legend|Archean|Archean|Age: 3125-3115Ma.    Basalt and calcalkaline volcanic rock.   Geological Province: Pilbara Craton||||||07-NOV-08
31020|Whundo Group|24353|3|Fully described|p1|Archean|Archean|Overlain by Cleaverville Formation. Age: 3130-3115 Ma. Max Thickness: 10km. Geological Province: Pilbara Craton||||||01-JUL-14
31020|Whundo Group|24541|3|Fully described|p11 Tb.2, p21-22|Archean|Archean|Geological Province: Central Pilbara Tectonic Zone. Age: 3130-3115 Ma. Overlain by Gorge Creek Group. Maximum Thickness: ~10km.||||||07-NOV-08
31020|Whundo Group|24543|5|Briefly described|Map legend|Archean|Archean|Of the Pilbara Supergroup.  Age: c.3120Ma.||||||07-NOV-08
31020|Whundo Group|24550|5|Briefly described|p36 Tb. 3.2|Archean|Archean|Calc-alkali felsic and mafic volcanics. Unconformably overlain by the Whim Creek Group. Age: 3120Ma. Geological Province: Pilbara Craton. See also p74 Tb. 5.1.||||||07-FEB-11
31020|Whundo Group|24590|6|Mentioned|p28 Fig. 1.2|||Geological Province: Pilbara Craton.||||||07-FEB-11
31020|Whundo Group|50300|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
31020|Whundo Group|50430|4|Described|p153||Archean|Age: 3130-3115 Ma. Predominantly basalt, interpreted to have been deposited on oceanic crust in post-3240 rift. In Sholl Domain.||||||07-NOV-08
31020|Whundo Group|60362|5|Briefly described|p1516-1518, p1528-1530, p1534|Archean|Archean|Basement to NW Mallina Basin. Geochemistry, Nd-isotopic compositions discussed: highest such values in any Pilbara Craton supracrustal sequence.|c.3.12 Ga.||||Dominantly tholeiitic basalts, but also basalts with calc-alkaline affinities, and up to 5% felsic rocks. Includes tonalite.|
31020|Whundo Group|61253|5|Briefly described|p50 Fig. 1, p52 Fig. 2|Archean|Archean|Age: ~3.12Ga.  Geological province: western Pilbara Craton.  See also p58.||||||07-NOV-08
31020|Whundo Group|63372|5|Briefly described|Map Legend|Archean|Archean|Of the Pilbara Supergroup. Geological Province: West Pilbara Granite-Greenstone Terrane. Age: 3115-3125Ma.||||||07-NOV-08
31020|Whundo Group|63441|4|Described|p5 Tb. 1, p14 Fig. 2, p24|Archean|Archean|Of Pilbara Supergroup. Comprises Nallana, Tozer, Woodbrook and Regal Formations and Bradley Basalt. Age: 3.12Ga. Thickness: ~10,000m. In the Sholl Terrane, West Pilbara Superterrane. Succession of mafic and felsic metavolcanic rocks.||||||07-FEB-11
31020|Whundo Group|63538|4|Described|p2 Fig. 1, p5, p7, p22-24, p26 Fig. 18|Archean|Archean|Overlain unconformably by Whim Creek Group. Age: 3120 Ma. Thick: >10000m. Geological Province: Pilbara Craton. Thick succession of bimodal basaltic to felsic volcanics and volcaniclastics rocks.||||||17-APR-13
31020|Whundo Group|63649|5|Briefly described|p200 Fig. 1|Archean|Archean|Geological Province: West Pilbara Terrane/ Sholl Terrane. Granitic rocks.||||||07-FEB-11
31020|Whundo Group|64174|5|Briefly described|Map legend|Archean|Archean|Includes Nallana and Tozer Formations, Bradley Basalt and Woodbrook Formation. Age ranges include: c.3125Ma, 3128-3118Ma, c.3115Ma and c.3117Ma.||||||07-NOV-08
31020|Whundo Group|64580|4|Described|map legend||Mesoarchean|Amphibolite derived from metabasalt; Ultramafic schist.||||||15-DEC-08
31020|Whundo Group|64632|5|Briefly described|p201, 202, 203, Fig.2, p205, 206, 207|Mesoarchean|Mesoarchean|Sholl Terane, West Pilbara Superterrane. > 10km thick. Compositionally distinct from Pilbara Supergroup rocks. Range of magma types with geochemical features similar to subduction-related magmas.|3130-3110 Ma||Nallana Formation, Tozer Formation, Bradley Basalt.|Unconformably overlain by the Whim Creek Group. Base intruded by granites.|Consists of bimodal basaltic to felsic volcanic and volcaniclastic rocks.|
31020|Whundo Group|66118|4|Described|p146 Fig.1, p154 Fig.9, p159 Fig.13,p160|||Pilbara Craton. West Pilbara Superterrane. Sholl Terrane. Interpreted to have been deposited in an intra-oceanic arc complex.|c. 3120 Ma Whundo Group and Railway Supersuite||||Tholeiitic basalts.|26-MAY-20
31020|Whundo Group|66217|5|Briefly described|p9, p38.|Mesoarchean|Mesoarchean|Sholl Terrane. Intra-oceanic arc.|3.13-3.11 Ga.|||||
31020|Whundo Group|67130|5|Briefly described|p13, p14 fig 9|Mesoarchean|Mesoarchean|Sholl Terrane. Rocks suggest formation in oceanic fore-arc.|3130 Ma  - 3110 Ma||||Bimodal basaltic to felsic volcanic and volcaniclastic rocks. Includes boninites, Nb-enriched basalts, adakites and rhyolites.|
31020|Whundo Group|67201|4|Described|p3, p7, p10-13, p15-24, see comments|Archean||In northwestern Pilbara Craton, West Pilbara Superterrane, Sholl Terrane, Whundo Basin. Regional unconformity at top; tectonic contact (Sholl Shear Zone) at base. No stratigraphic base is exposed, but is interpreted to have been deposited above c. 3200 Ma oceanic crust, in an oceanic arc setting. Exceptional amongst Mesoarchean and Paleoarchean volcanic sequences in that it preserves compelling evidence of modern-style subduction processes. Detailed chemostratigraphic analysis. Three volcanic packages. Age also shown as 3130-3115 Ma. Nd-isotopic compositions represent juvenile crustal addition, with values close to depleted mantle values. Unconformably underlies units of Mallina Basin. Where Mount Roe Basalt is absent, Hardey Formation unconformably rests on irregular paleosurface composed of Whundo Group, Cleaverville Formation, and Whim Creek Group. Lithology description continued: Deformed, metamorphosed; greenschist facies, little primary mineralogy preserved (though textures commonly preserved). Page location continued: p26-27, p42, p45-49, p60-61, p63-64, p67.|3126-3112 Ma (Hickman et al. 2006)||Woodbrook Formation, Bradley Basalt, Tozer Formation, Nallana Formation|Faulted against Regal Formation. Is intruded by Railway Supersuite; also thrust over Cheratta Granitic Complex. Unconformably underlies Gorge Creek and Fortescue Groups.|Bimodal volcanics. Includes boninites, interlayered tholeiitic and calc-alkaline volcanics, Nb-enriched basalts, adakites, and greenstones. Upper volcanic package includes felsic volcanics and volcaniclastic units. See comments|25-NOV-16
31020|Whundo Group|67269|6|Mentioned|p2 Fig.1|Paleoarchean|Paleoarchean|Sholl Terrane, W. Pilbara Superterrane.||||||
31020|Whundo Group|68035|4|Described|p289, 290, 294, p285 Fig 2, p290 Fig 5|Mesoarchean|Mesoarchean|Sholl Terrane, West Pilbara Superterrane. 10 km thick. Locally contains economic VHMS Cu-Zn mineralisation.|3130 - 3110 Ma|||Sheared contact with Railway Supersuite. Unconformably overlain by Gorge Creek Group.|Lower package: calc-alkaline + boninite-like rocks. Middle package: tholeiitic rocks; minor boninite-like rock, rhyolite. Upper package: calc-alkaline rocks, including adakite, basalt and rhyolite. Rare chert, BIF, quartzite.|
31020|Whundo Group|68284|6|Mentioned|p2|Archean|Archean|West Pilbara Superterrane.|||||Granitic rocks.|
31020|Whundo Group|69185|5|Briefly described|GEOL_LUT_CSV files||Mesoarchean||||Includes Bradley Basalt, Nallana Formation, Tozer Formation, Woodbrook Formation.||Ultramafic schsit; amphibolite derived from metabasalt.|
31020|Whundo Group|69299|3|Fully described|p1,4,p6 Tb.1,7,p8 Fig.5,9,11-14,18,21,22|Archean|Archean|Of Mesoarchaean West Pilbara Granite-Greenstone Terrane. Thickness: about 10 km. Small sub-economic Ni-Cu deposits. Outcrops in northwestern corner of COOYA POOYA. At base, tectonic contact along Maitland Shear Zone. High-angle regional unconformity with overlying Whim Creek Group constituent units on COOYA POOYA. Greenstones of Whundo Group (Hickman 1997) on COOYA POOYA were mapped lithologically rather than stratigraphically, and no age relationships are implied by vertical arrangement of units bracketed as 'Pilbara Supergroup, no stratigraphic subdivision in map legend'. Zircon age from granitoid of Wundo Group.|c. 3130-3115 Ma; 3127 +/- 8 Ma zircon Nelson 2001|Of Pilbara Supergroup.|Includes Tozer Formation, Nallana Formation.|Contact with Cheratta Granitoid Complex is partly tectonic (faulted) and partly intrusive; is unconformably overlain by Mount Roe Basalt.|Volcanic; dominantly basaltic; metamorphosed.|
31020|Whundo Group|69300|5|Briefly described|map legend|Archean|Archean|West Pilbara Granite-Greenstone Terrane||Pilbara Supergroup|Woodbrook Formation, Bradley Basalt, Nallana Formation|||
31020|Whundo Group|69301|4|Described|p3-6, p9 Tb.1, p14-15|||Pilbara Craton. West Pilbara Superterrane. Whundo Basin. Sholl Terrane. Interpreted to be composed of intra-oceanic arc volcanics. Divided into four lithostratigraphic formations. Exposed basal contact is Maitland Shear Zone (which prior to deformation was a low-angle thrust). Northern contact is defined by Sholl Shear Zone.|3126-3118 Ma from unit ages||Woodbrook Formation, Bradley Basalt, Tozer Formation, Nallana Formation|Sholl Shear Zone at base. Is unconformably overlain (without any angular discordance) by Gorge Creek Group.|Granitic rocks.|
31020|Whundo Group|69740|5|Briefly described|p651, 663-665, 672-673, 676|Mesoarchean|Mesoarchean|Pilbara Craton. Suprasubduction zone-type ophiolite; backarc to forearc setting. Also appears as Whundo complex. Stratigraphic columnar section.|3.12 Ga.||||Boninites, interlayered tholeiites, and calc-alkaline volcanic rocks.|
31020|Whundo Group|70022|6|Mentioned|p114-115|||Sholl Terrane, West Pilbara Superterrane.|3130-3110 Ma.|De Grey Supergroup.|Nallana, Tozer, Woodbrook Formations; Bradley Basalt.|||
31020|Whundo Group|70775|5|Briefly described|iv, p6, p10, p12-p13, p15|Mesoarchean|Mesoarchean|Whundo Basin, Sholl Terrane. This group is up to 10km thick. Hosts subduction related VHMS Cu-Zn(-Pb-Ag) deposits. See also p19, p25, p32-p34, p36-p38, p41, p44 fig 27, p47, p50, p52-p53, p57, p61, p64-p65, p70, p72, p74-p75, p81, p99.|c. 3130-3110 Ma||Includes the Nallana Formation, Tozer Formation, Bradley Basalt and the Woodbrook Formation.|Unconformably overlain by the Cleaverville Formation. Unconformably overlain by the Gorge Creek Group. Faulted against the Railway Supersuite. Intruded by the Maitland River Supersuite.|Mafic and felsic lavas and felsic volcaniclastic rocks.|
31020|Whundo Group|70826|6|Mentioned|p6 tbl 2|Mesoarchean|Mesoarchean|Whundo Basin.||||Is intruded by the Railway Supersuite.||
31020|Whundo Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||basalt, dolerite, ash tuff, chert|
31020|Whundo Group|71349|6|Mentioned|p738|Archean|Archean|Coeval with Railway Supersuite.|c.3.1 Ga.|||||
31020|Whundo Group|71803|6|Mentioned|p381||||ca 3120 Ma|||||
31020|Whundo Group|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Whundo Basin.|||Includes Woodbrook Formation, Bradley Basalt, Tozer Formation, Nallana Formation.||Mafic and felsic volcanic rocks; local ultramafic rocks and chert; metamorphosed.|
31020|Whundo Group|72251|5|Briefly described|p52,54|Mesoarchean|Mesoarchean|Geological province: Sholl Terrane, West Pilbara Superterrane, Pilbara Craton.|3130-3110 Ma||Includes Nallana Formation.|Overlain unconformably by Gorge Creek Group. Underlain by Regal Formation.||
31020|Whundo Group|72668|4|Described|p1-p4, p7-8, p11-14, p16,21,22,25,28,30|||Sholl Terrane. Is a fault bounded, >10km thick succession with geochemical characteristics of modern oceanic arcs. Neither the base nor the top of the group is preserved and is interpreted to represent juvenile crust. Contemporaneous with the granitic gneisses of the Railway Supersuite. Geochemistry is described. See also p20, p21, p28, p29, p30.|c. 3130-3110 Ma||Includes the Nallana Formation, Tozer Formation, Bradley Basalt and the Woodbrook Formation.|Coeval with the Railway Supersuite.|Bimodal basaltic to felsic volcanic and volcaniclastic rocks.|14-JAN-22
68515|Whyjabby Granodiorite|63441|2|Defined|p10 Tb. 2, p37|Archean|Archean|Of the Maitland River Supersuite. Age: 2994+/-2Ma. Geological province: Pilbara Craton.||||||07-FEB-11
68515|Whyjabby Granodiorite|64174|5|Briefly described|Map legend|Archean|Archean|Of the Maitland River Supersuite. Geological province: Pilbara Craton.  Foliated microcline-porphyritic hornblende granodiorite; local xenoliths of tonalite gneiss; metamorphosed.||||||07-NOV-08
68515|Whyjabby Granodiorite|64580|4|Described|map legend||Mesoarchean|Of Maitland River Supersuite. Folated, microcline porphyritic hornblende granodiorite; locally contains xenoliths of tonalite gneiss; metamorphosed.||||||15-DEC-08
68515|Whyjabby Granodiorite|67201|5|Briefly described|p16-17 Fig.9|Archean|Archean|Pilbara Craton. In Roebourne-Karratha area.||Maitland River Supersuite|||Foliated, microcline-porphyritic hornblende granodiorite; local xenoliths of tonalite gneiss; metamorphosed.|
68515|Whyjabby Granodiorite|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Maitland River Supersuite.|||Foliated, microcline porphyritic hornblende granodiorite; locally contains xenoliths of tonalite gneiss; metamorphosed|
68515|Whyjabby Granodiorite|70775|5|Briefly described|p15, p53|Mesoarchean|Mesoarchean|Pilbara Craton. Together with the Jean Well Granodiorite, Toorare Tonalite, Brill Monzogranite, Waloo Waloo Monzogranite and Mardeburra Granodiorite comprises the Cherratta Granitic Complex. Excellent exposures occur in the type area of Baynton Hill, close to Karratha Homestead.|2994 +/- 2 Ma (SHRIMP, Nelson, 1997f)|Maitland River Supersuite|||Foliated, microcline-porphyritic hornblende granodiorite, local xenoliths of tonalite gneiss; metamorphosed.|
68515|Whyjabby Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite|
68515|Whyjabby Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|De Grey Superbasin.|2994+/-2 Ma.|Maitland River Supersuite|||Hornblende granodiorite; microcline phenocrysts; foliated and with local xenoilths of tonalite gneiss; metamorphosed.|
31144|Wicherina Sandstone Member|23279|6|Mentioned|Fig2 p3||Asselian|||||||07-JAN-10
31144|Wicherina Sandstone Member|43495|4|Described|6-25||Asselian|||||||
31144|Wicherina Sandstone Member|61811|5|Briefly described|p66.|Carboniferous|Carboniferous|Northern Perth Basin. See also references to Wicherina Member (p3 Fig.2, p23). Type section details in Appendix 1.||Unit in Nangetty Formation.|||Includes massive, rippled, contorted and pebbly sandstone.|
26213|Wickham Formation|14019|3|Fully described|p14-15|||Basal unit of the Wattie Group. Sandstone, minor chert and conglomerate. Unconformably overlies Killaloc Formation; progressively overlies younger formations of Limbunya Group from east to west. Min. thickness: 315m. Geological Province: Victoria Basin.||||||
26213|Wickham Formation|24122|5|Briefly described|p4 Fig.3|||Of Wattie Group.  Geological Province: Victoria Basin.||||||
26213|Wickham Formation|24297|3|Fully described|p5|Proterozoic|Proterozoic|Of Wattie Group. Conformably overlain by Burtawurta Formation, unconformably overlies Limbunya Group. 176m thick at type section.  Geological Province: Victoria Basin.  See also p5 Tb. 2.||||||
26213|Wickham Formation|24298|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Wattie Group. Quartz sandstone.||||||19-DEC-06
26213|Wickham Formation|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Wattie Group.  Unconformably overlies the Killaloc Formation; overlain by Burtawurta Formation. Geological Province: Victoria Basin.||||||25-JAN-06
26213|Wickham Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Wattie Group. Geological Province: Victoria Basin.||||||
26213|Wickham Formation|28255|3|Fully described|p33, Tb. 11 (op.. p8)|Adelaidean|Adelaidean|Basal unit of the Wattie Group. Consists of sandstone and conglomerate with subordinate siltstone and chert. Unconformably overlies several units of the Limbunya Group; conformably overlain by Burtawurta Formation. Max. thickness: 155m. See also p122 App.||||||
26213|Wickham Formation|30003|4|Described|p8, p12|||Basal unit of the Wattie Group.  Unconformably overlies the Limbunya Group. Carpentarian or Adelaidean.||||||19-APR-05
26213|Wickham Formation|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
26213|Wickham Formation|32172|4|Described|Table 1|||Carpentarian or Adelaidean||||||
26213|Wickham Formation|32173|5|Briefly described|Map legend|Adelaidean|Carpentarian|Of the Wattie Group.  Feldspathic sandstone, laminated and brecciated chert interbeds.  Carpentarian or Adelaidean (per legend).||||||17-NOV-04
26213|Wickham Formation|32175|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Wattie Group.  Massive and blocky fine and medium quartz sandstone.||||||02-DEC-04
26213|Wickham Formation|32660|5|Briefly described|Table 6|||||||||
26213|Wickham Formation|33374|6|Mentioned|p7|||See also p9. Strat. table.||||||19-DEC-06
26213|Wickham Formation|33375|5|Briefly described|p7, p9 Tb. 1|||Of the Wattie Group. Overlain by the Burtawurta Formation.||||||26-APR-05
26213|Wickham Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26213|Wickham Formation|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Wattie Group.  Massive quartz sandstone, laminated and brecciated chert interbeds.||||||27-APR-05
26213|Wickham Formation|45112|5|Briefly described|Table 7|||||||||
26213|Wickham Formation|48943|2|Defined|p40|Adelaidean|Adelaidean|Strat. section p133.||||||07-NOV-16
26213|Wickham Formation|60589|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Wattie Group.  Quartz sandstone.  Unconformably overlies the Killaloc Formation of the Limbunya Group.  Geological Province: Victoria Basin.||||||
26213|Wickham Formation|60672|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Quartz Sandstone, micaceous stilstone and chert, basal conglomerate. Of Wattie Group. Unconformably overlies Limbunya Group. Overlain by Burtawurta Formation. Geological Province: Victoria Basin.||||||11-JAN-05
26213|Wickham Formation|60685|4|Described|p4 Fig. 3, p5|Paleoproterozoic|Paleoproterozoic|Of the Wattie Group. Fine to medium grained sandstone. Unconformably overlies Limbunya Group; conformably overlain by Burtawurta Formation. Max. Thickness: 176m in WAVE HILL. Geological Province: Victoria Basin.||||||07-NOV-08
26213|Wickham Formation|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Wattie Group.||Is overlain by Burtawurta Formation.||
26213|Wickham Formation|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Wattie Group.||Unconformably overlies Campbell Springs Dolostone and Fraynes and Killaloc Formations. Is overlain by Burtawurta Formation.|Massive quartz sandstone, laminated and brecciated chert interbeds.|
26213|Wickham Formation|68733|5|Briefly described|p177-184||Statherian|Sweet et al. (1974). Previously included in the Victoria Basin by Cutovinos et al. (2002). Now included in the Birrindudu Basin due to a recent subdivision by the NGTS (Dunster and Ahmad 2013). Maximum depositional age of ca. 1639 +/- 16 Ma|Maximum depositional age of ca. 1639 +/- 16 Ma|Basal unit of the Wattie Group.||Unconformably underlain by the Limbunya Group. Conformably overlain by the Burtawurta Formation.|Thick bedded, red-purple ferruginous medium-grained feldspathic sandstone.|06-DEC-17
26213|Wickham Formation|69432|4|Described|p17:2, 9|||Birrindudu Basin. 175m thick. Detrital zircon maximum depositional age.|<1639 +/- 16 Ma (Carson, 2010).|Wattie Group.||Unconformably overlies several Limbunya Group units. Is overlain conformably by Burtawurta Formation or Hughie Sandstone.|Fine to medium, moderately well-sorted immature sandstone, conglomerate and chert, and rare siltstone; basal conglomerate common. Local cauliflower chert, ripple marks and mudcracks.|12-JUL-16
26213|Wickham Formation|69673|6|Mentioned|p48 fig 35|||Age is maximum depositional age.|1639 +/- 16 Ma|Wattie Group||Unconformably overlies Killaloc Formation, overlain by Burtawurta Formation||
26213|Wickham Formation|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.||Shown as base of Wattie Group.||Unconformably overlies Campbell Springs Dolostone, Blue Hole Formation, Fraynes and Killaloc Formations. Is overlain by Burtawurta Formation.|Massive quartz sandstone, laminated and brecciated chert interbeds.|
26213|Wickham Formation|70848|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Victoria Basin.||Wattie Group.|||Basal conglomerate, pebbly sandstone, chert, quartzite, quartz sandstone, siltstone, medium-thick bedded.|
26213|Wickham Formation|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Wattie Group.||Unconformably overlies Fraynes Formation (Limbunya Group). Is overlain by Burtawurta Formation.|Quartz sandstone, micaceous siltstone and chert, basal conglomerate.|21-SEP-17
26213|Wickham Formation|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Wattie Group.||Unconformably overlies Limbunya Group. Is overlain by Burtawurta Formation.|Quartz sandstone, micaceous siltstone and chert; local basal conglomerate.|
26213|Wickham Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
26213|Wickham Formation|71302|5|Briefly described|p6,72,74||Paleoproterozoic|Of Birindudu Basin. Maximum depositional age: 1639+\-16 Ma (Carson, 2013; Munson, 2016 and Munson, in prep).||Unit of Wattie Group.||Overlain by Burtawurta Formation. Underlain by Killaloc Formation.||
26213|Wickham Formation|71592|5|Briefly described|Appendix A.|||Victoria River Region.|1639+/-16 Ma (MDA: Pb/Pb zircon).||||Sandstone.|
26213|Wickham Formation|72718|6|Mentioned|p7|Statherian[?]|Statherian|Birrindudu Basin.|1639 +/- 16 Ma|Wattie Group||Unconformably[?] underlain by Killaloc Formation (Limbunya Group). Overlain by Burtawurta Formation.||
26213|Wickham Formation|73083|6|Mentioned|p30-31|||||Wattie Group||Unconformably underlain by Limbunya Group.||
73852|Wickham Pillow Basalt|24391|5|Briefly described|p8-4 Fig.2|Archean|Archean|Of Point Samson Group. Alterated pillowed matebasite, dolerite dykes. Geological Province: Pilbara Block.||||||07-NOV-08
31795|Wilagee intrusion|43854|5|Briefly described|Map Legend||Proterozoic|||||||
31795|Wilagee intrusion|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31795|Wilagee intrusion|60498|6|Mentioned|p1020.|Paleoproterozoic|Paleoproterozoic|No lithology was stated for the stratigraphic name. A mafic - ultramafic intrusion. Electron microprobe geochemical analyses of apatites are detailed.||||||
31795|Wilagee intrusion|63866|5|Briefly described|p133|||Western Zone, Halls Creek Orogen.||||||
31795|Wilagee intrusion|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Layered mafic-ultramafic intrusions; peridotite, troctolite, gabbro, olivine gabbro, olivine gabbronorite, gabbronorite, leucogabbro, and anorthosite; minor chromitite layers.||||||15-DEC-08
31795|Wilagee intrusion|69099|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|Grouped as Springvale, Wilagee, and Foal Creek intrusions, with a single lith description in 500k_geologyp08_lut.csv.|||||Layered mafic-ultramafic intrusions; peridotite, troctolite, gabbro, olivine gabbro, olivine gabbronorite, gabbronorite, leucogabbro, and anorthosite; minor chromitite layers.|04-AUG-15
31795|Wilagee intrusion|69634|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|Grouped with Springvale and Foal Creek intrusions.|||||Layered mafic-ultramafic intrusions; peridotite, troctolite, gabbro, olivine gabbro, olivine gabbronorite, gabbronorite, leucogabbro, and anorthosite; minor chromitite layers.|
31795|Wilagee intrusion|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Layered mafic-ultramafic intrusion; gabbro, leucogabbro, leucogabbronorite, gabbronorite, anorthosite, minor troctolite; some olivine and/or chromitite-bearing; in rhythmic cycles; peridotite and troctolite|
29216|Wilcox Formation|6876|6|Mentioned|p100 Fig.5.|Paleogene|Paleogene|||||||
29216|Wilcox Formation|23726|5|Briefly described|p8 Fig 2c|Eocene||Underlying unit Dockrell Formation. Geological Province: Carnarvon Basin.||||||
29216|Wilcox Formation|40617|5|Briefly described|p16|||||||||
29216|Wilcox Formation|40800|2|Defined|p20|middle Eocene|early Eocene|Early to Middle Eocene||||||30-JUN-14
29216|Wilcox Formation|41271|3|Fully described|p170|||||||||
29216|Wilcox Formation|41437|6|Mentioned|p66|||||||||
29216|Wilcox Formation|41439|5|Briefly described|p123|||||||||
29216|Wilcox Formation|41732|6|Mentioned|Fig.3|||||||||
29216|Wilcox Formation|42116|5|Briefly described|Fig.1 P6|||||||||
29216|Wilcox Formation|43712|6|Mentioned|Fig.10,p52||Eocene|||||||
29216|Wilcox Formation|43724|6|Mentioned|Fig.15,p65||Eocene|||||||
29216|Wilcox Formation|61155|5|Briefly described|p15|Early Eocene|Late Paleocene|Age: 58-52Ma. Max. thickness: 160m. Geological Province: Carnarvon Basin /offshore.||||||
29216|Wilcox Formation|62734|5|Briefly described|p1362 Fig. 2|Eocene|Eocene|Geological Province: Barrow Sub-basin.||||||01-SEP-08
29216|Wilcox Formation|62837|5|Briefly described|Stratigraphic columns|Eocene|Eocene|Age: 55-50Ma. Geological Province: Dampier Sub-basin, Rankin Platform and Beagle Sub-basin.||||||
29216|Wilcox Formation|63950|5|Briefly described|p336 Fig. 4|Eocene|Paleocene|Overlies Dockrell Formation; underlies Walcott Formation. Geological Province: northern Carnarvon Basin.||||||30-JUN-14
29216|Wilcox Formation|67200|5|Briefly described|p8 fig 6, p53|Pliocene|Eocene|Thermal conductivity of 1.23 W/mK||||Overlies Dockrell Formation,|Crudely bedded limestone and marl.|
29216|Wilcox Formation|67368|6|Mentioned|p209 Fig.4.|Early Eocene|Paleocene|||||||
29216|Wilcox Formation|67970|6|Mentioned|p25 Fig.4.|Ypresian|Ypresian|Exmouth Plateau.||||||
29216|Wilcox Formation|69692|6|Mentioned|p4|Eocene|Eocene|Northern Carnarvon Basin.||||Overlies Dockrell Formation. Is overlain by Walcott Formation.||
29216|Wilcox Formation|70066|5|Briefly described|Dampier: Fig.2. Exmouth: Fig.2|Ypresian|Ypresian|See also Regional: Fig.6. Northern Carnarvon Basin.||||Overlies Dockrell Formation. Is overlain by Giralia Calcarenite and Walcott Formation.||
29216|Wilcox Formation|70906|5|Briefly described|p757-758|Eocene|Eocene|Gorgon Platform.||||Overlies Dockrell Formation. Is overlain by Walcott Formation.||
31058|Wild Dog Creek Gabbro|22474|6|Mentioned|p20|||||||||
31058|Wild Dog Creek Gabbro|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  In the Bow River batholith.  Age: 1835-1805Ma.||||||07-NOV-08
31058|Wild Dog Creek Gabbro|43854|5|Briefly described|Map Legend||Proterozoic|||||||
31058|Wild Dog Creek Gabbro|43931|6|Mentioned|p20|||||||||
31058|Wild Dog Creek Gabbro|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31058|Wild Dog Creek Gabbro|60283|6|Mentioned|p27 Fig.4||||||||Voluminous gabbro.|
31058|Wild Dog Creek Gabbro|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Sally Downs Supersuite|||Magnetite gabbro and magnetite-quartz gabbronorite with veins of intermediate hybrid rock; basic and intermediate hybrid rocks cut by veins of biotite granite.|04-AUG-15
31058|Wild Dog Creek Gabbro|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Sally Downs Supersuite|||Magnetite gabbro and magnetite quartz gabbronorite with veins of intermediate hybrid rock; basic and intermediate hybrid rocks cut by veins of biotite granite.|
31058|Wild Dog Creek Gabbro|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2.|1832-1808 Ma (Inferred)|Unit of Sally Downs Supersuite.|||Magnetite gabbro and magnetite-quartz gabbronorite with veins of intermediate hybrid rock; basic and intermediate hybrid rocks cut by veins of biotite granite|
31058|Wild Dog Creek Gabbro|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1808-1832 Ma|Sally Downs Supersuite|||Magnetite gabbro and magnetite-quartz gabbronorite with veins of intermediate hybrid rock.|
31058|Wild Dog Creek Gabbro|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1832-1808 (inferred)|Unit of Sally Downs Supersuite.|||Magnetite gabbro and magnetite-quartz gabbronorite with veins of intermediate hybrid rock; basic and intermediate hybrid rocks cut by veins of biotite granite|
79819|Wildcat Gabbro|69586|5|Briefly described|p11-12|||Beardsmore (2002). Hosts significant gold mineralisation (eg Sunrise Birthday deposit, described in some detail). Crops out as dark brown ridges.||||||
79819|Wildcat Gabbro|71212|5|Briefly described|intro p2, p59,  p46, p52, p53|||Yilgarn Craton. One of 5 informal units that are together equivalent to the formal Bounty Igneous Complex. Up to 400m thick. Outcrop characteristics discussed. See also p89, p105, p106, p108, p199, p213, p216.||||Intrudes the Never Can Tell Basalt. Overlies the Mikado Gabbro.||26-SEP-17
74872|Wilgie Mia Formation|64891|5|Briefly described|p37 Fig. 2, p39, p48-9 Tb. 1|Archean|Archean|Of the Polelle Group. Conformable on Greensleeves Formation. Age: c. 2750Ma. Geological province: Murchison Domain. BIF and felsic volcaniclastic rocks; weakly metamorphosed.||||||07-FEB-11
74872|Wilgie Mia Formation|65546|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Polelle Group, Youanmi Terrane, Yilgarn Craton. Unnamed units of quartzite and banded iron-formation and ferruginous-banded chert; minor jaspillite and haematite-rich rock; minor volcaniclastic sandstone; metamorphosed.||||||
74872|Wilgie Mia Formation|65548|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Polelle Group, Youanmi Terrane, Yilgarn Craton. Age dates: <2969 Ma, 2752 Ma. Schistose pelite, psammite; banded iron-formation, ferruginous-banded chert; minor jaspilite and haematite-rich rock; minor volcaniclastic sandstone; metamorphosed.||||||25-FEB-13
74872|Wilgie Mia Formation|66195|5|Briefly described|p605|||In the Polelle Group. Felsic volcaniclastics and banded iron formations.||||||13-MAR-12
74872|Wilgie Mia Formation|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Mapped as seven separate but un-named units|2752 - 2735 Ma.|Unit in Polelle Group.|||Quartz-porphyritic rhyolite; banded iron-formation and ferruginous banded chert; quartz-rich sandstone; mudstone, siltstone and sandstone, weakly metamorphosed; schistose pelite and psammite.|
74872|Wilgie Mia Formation|67129|4|Described|p18 Fig.19, p20, p24-25, p29, p39,p41-42|Archean|Archean|Murchison Domain, Youanmi Terrane. The type area is in the Weld Range. Isotopic data shows that the jaspilitic precursor was precipitated abiogenically.|2790-2740 Ma|Polelle Group||Is interbedded with Greensleeves Formation. Unconformably overlain by Ryansville Formation; intruded by Gnanagooragoo Igneous Complex.|Banded iron-formation, jaspilitic cherts, green-black shale, layered red and white chert. Jaspilitic (hematite-bearing) chert alternates with pure magnetite at the type area.|07-SEP-17
74872|Wilgie Mia Formation|68110|5|Briefly described|p673-674, Fig. 2.|Neoarchean|Neoarchean|Murchison Domain.|c. 2734 Ma|Of the Polelle Group.||Conformably overlies Greensleeves Formation.|BIF, felsic volcaniclastic rocks.|
74872|Wilgie Mia Formation|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. Volcaniclastic breccia U-Pb zircon maximum age: 2979 +/- 3 Ma as the magmatic crystallization age of the rhyolite from which the sampled clast was derived. From geochron file 193972.1.pdf.||Polelle Group|Includes 10 unnamed subunits.|Conformably overlies Greensleeves Formation. Unconformably overlain by Ryansville Formation (Glen Group).|Schistose pelite and psammite; Mudstone, siltstone and sandstone; Foliated meta banded iron-formation; Banded iron-formation and ferruginous banded chert; Polymictic breccia; Felsic volcanic and volcaniclastic rock; Quartz-porphyritic rhyolite.|23-OCT-15
74872|Wilgie Mia Formation|68698|5|Briefly described|p4-5, p9, p11|Neoarchean|Neoarchean|Includes a c.2750 Ma felsic volcanic rock which includes a rhyolite clast containing c.2980 Ma zircons.|c.2760-2735 Ma.|Polelle Group.||Overlies Greensleeves Formation. Is overlain unconformably by Ryansville Formation (Glen Group). Is intruded by the coeval Gnanagooragoo Igneous Complex.|Interbedded BIF, shale and felsic volcaniclastic rocks.|
74872|Wilgie Mia Formation|69583|4|Described|p47, p49, p126; Plate 2|Neoarchean|Neoarchean|Weld Range, Murchison Domain. Coeval with emplacement of Gnanagooragoo Igneous Complex below and within the BIF component of this unit. Age given also as c.2785 Ma.|c.2760-2740 Ma.|Topmost Polelle Group.||Overlies and is intruded by Gnanagooragoo Igneous Complex. Is overlain unconformably by Ryansville Formation.|Interbedded BIF, shale and felsic volcaniclastic rocks; metamorphosed.|
74872|Wilgie Mia Formation|69584|5|Briefly described|p5 Fig.2|Neoarchean|Neoarchean|||Polelle Group||Unconformably overlain by the Ryansville Formation, overlies the Greensleeves Formation.||
74872|Wilgie Mia Formation|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Polelle Group.||||
74872|Wilgie Mia Formation|70020|4|Described|p117-118|Neoarchean|Neoarchean|Geological province: Yilgarn Craton.||Unit of Polelle Group.||Overlain by Ryansville Formation/Glen Group. Underlain by Greensleeves Formation.|Interbedded BIF, shale and felsic volcaniclastic rocks.|
74872|Wilgie Mia Formation|70030|5|Briefly described|p190,192|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton.||Unit of Polelle Group.||Uppermost unit of Polelle Group. Overlain by Ryansville Formation/Glen Group. Underlain by Greensleeves Formation.|Dolerites.|
74872|Wilgie Mia Formation|70418|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c.2748 Ma.|Polelle Group.|||Metamorphosed felsic volcanic and volcaniclastic rocks, commonly deeply weathered and kaolinised; foliated metamorphosed BIF, commonly with magnetite crystals; schistose pelite and psammite with local biotite porphyroblasts.|
74872|Wilgie Mia Formation|70796|5|Briefly described|100k_geologyl_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv,  500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 155568.1.pdf, 155569.1.pdf, 155572.1.pdf, 183338.1.pdf, 185922.1.pdf, 185926.1.pdf, 185927.1.pdf, 185932.1.pdf, 193972.1.pdf, 197420.1.pdf, Cue100_2443_stratig.pdf, Koonmarra100_2445_stratig.pdf, Madoonga100_2444_stratig.pdf, MountMagnet100_2441_stratig.pdf. Numerous additional lithologies are discussed. Unconformably overlies the Thundelarra Supersuite.|ca 2790  2735 Ma (inferred)|Polelle Group||Conformably overlies the Greensleeves Formation. Unconformably overlain by the Ryansville Formation. Intruded by the Yalgowra Suite.|Schistose pelite and psammite with local biotite porphyroblasts, quartzite, metachert, foliated metamorphosed banded iron formation and felsic volcanic and volcaniclastic rocks.|
74872|Wilgie Mia Formation|70830|5|Briefly described|p5, p7, p9||||2760-2740 Ma|Polelle Group||Overlies the Greensleeves Formation. Intruded by the Gnanagooragoo Igneous Complex.|Interbedded banded-iron formation, shale and felsic volcaniclastic rocks.|
74872|Wilgie Mia Formation|71168|4|Described|p7-p8|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c. 2750-2740 Ma|Polelle Group||Overlies the Greensleeves Formation. Unconformably overlain by the Ryansville Formation (Glen Group).|Interbedded banded-iron formation, shale and felsic volcaniclastic rocks.|
74872|Wilgie Mia Formation|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). Consists of a basal unit of ~1km thick layer of felsic volcaniclastic rocks, interbedded with about 300 m of BIF, and overlain by up to 4 km of BIF with thin volcaniclastic horizons (Van Kranendonk and Ivanic, 2009). Previously geochronological analysis include an interpreted max depositional age of 2752+\-9 Ma for a felsic volcaniclastic rock (Wang 1998), and interpreted magmatic age of 2741+\-7 Ma for a porphyritic monzogranite (Wingate et al., 2011). Sample GSWA155568 (metasiltstone; this study) yielded a weighted mean Pb/Pb age of 2792+\-9 Ma, interpreted to be maximum depositional age, and magmatic age of volcanics from the volcaniclastic component. Sample GSWA155572 (volcaniclastic metasandstone; this study) yielded a weighted mean Pb/Pb age of 2747+\-4 Ma, interpreted to be maximum depositional age of the sedimentary protolith. Sample GSWA 193972 (weathered felsic volcanic) yielded a weighted mean 207Pb/206Pb date of 2979+\-3 Ma, interpreted as the magmatic crystallization age of the rhyolite from which the sampled clast was derived. Sample GSWA 205717 (felsic schist) yielded a weighted mean 207Pb/206Pb date of 2948+\-3 Ma, interpreted as the magmatic crystallization age of the felsic volcanic protolith. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeol_lut.csv.|2790-2735 Ma|Unit of Poelle Group.||Overlain unconformably by Ryansville Formation. Underlain conformably by Greensleeves Formation. Intruded by Yalgowra Suite sills.|Schistose pelite and psammite with local biotite porphyroblasts; foliated metamorphosed BIFs and Fe-banded cherts; mudstone, siltstone, sandstone, felsic volcanics and volcaniclastics, quartz porphyritic rhyolite.|
74872|Wilgie Mia Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Youanmi Terrane.||Polelle Group|||Banded iron-formation and felsic volcaniclastic rocks; weakly metamorphosed.|
74872|Wilgie Mia Formation|72494|5|Briefly described|p15|||Youanmi Terrane, Yilgarn Craton.||Polelle Group.||Conformably overlies Greensleeves Formation. Is overlain by the Glen Group.|BIF and felsic volcaniclastic rocks.|
74872|Wilgie Mia Formation|73596|6|Mentioned|p1165|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane.|c.2750-2735 Ma.|Polelle Group.|||Includes BIF.|
39509|Wilina Granodiorite|63417|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite.  Age: 3324-3310Ma. Geological Province: Pilbara Craton. Quartz-rich biotite granodiorite and trondhjemite; medium-grained; weakly foliated; metamorphosed.||||||07-NOV-08
39509|Wilina Granodiorite|63441|5|Briefly described|p8 Tb. 2|Archean|Archean|Of Emu Pool Supersuite. Ages: 3324+/-6Ma and 3323+/-9Ma. Geological province: Pilbara Craton.||||||07-FEB-11
39509|Wilina Granodiorite|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.|c.3324 Ma (Wyatt et al. 2001).|Of Mount Edgar Granitoid Complex.|||Quartz-rich biotite granodiorite and trondhjemite; medium-grained, weakly foliated; biotite monzogranite, medium-grained, foliated.|
39509|Wilina Granodiorite|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c.3324 - 3310 Ma (Kloppenburg 2003).|Of Emu Pool Supersuite.|||Quartz-rich biotite granodiorite and trondhjemite; medium-grained, weakly metamorphosed.|
39509|Wilina Granodiorite|65827|2|Defined|p6 Tb.2, p13 Tb.4, p16, p18, p22, p59|Paleoarchean|Paleoarchean|New name. Formerly Wilina Pluton (Collins et al. 1998; Sims and Carson, 2001). A 10 km diameter oval intrusion around Wilina Well. 3324+/-6 Ma (SHRIMP U-Pb zircon; Collins et al. 1998) to 3310+/-10 Ma (SHRIMP U-Pb zircon; Nelson 2005). Of Emu Pool Supersuite. Weakly foliated, light pink-grey, medium- to coarse-grained biotite granodiorite and trondhjemite. Intrudes Duffer Formation, Apex Basalt, Underwood Gneiss. Post-dates Limestone Shear Zone.||||||
39509|Wilina Granodiorite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Age derived from sample of foliated biotite granodiorite (169042.1.pdf) - note there are two possible ages given in the document which may be the time of crystallization|3323 +/-9 Ma (SHRIMP)|Emu Pool Supersuite|||Quartz-rich biotite granodiorite and trondhjemite; medium grained; weakly metamorphosed|
39509|Wilina Granodiorite|69566|6|Mentioned|p236|||Mount Edgar Granitoid Complex, East Pilbara Granite-Greenstone Terrane.||Emu Pool Supersuite.||||
39509|Wilina Granodiorite|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA 169042 (biotite granodiorite) yielded an interpreted igneous crystallisation age of 3310+\-8 Ma for the monzogranite (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv.|3324-3310 Ma (inferred)|Unit of Emu Pool Supersuite.|||Quartz-rich biotite granodiorite and trondhjemite; medium grained; weakly metamorphosed|
39509|Wilina Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite, trondhjemite|
39509|Wilina Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||Max age 3324+/-6 Ma, min 3310+/-8 Ma.|Emu Pool Supersuite|||Quartz-rich biotite granodiorite and trondhjemite; medium grained; weakly metamorphosed.|
37330|Wilki Formation|23414|5|Briefly described|Map Legend|Neoproterozoic|Mesoproterozoic|Of Lamil Group, Yeneena Basin||||||
37330|Wilki Formation|23758|4|Described|p10|Neoproterozoic|Neoproterozoic|Previously Wilki Quartzite. Of Lamil Group. Geological Province: Yeneena Basin.||||||
37330|Wilki Formation|60470|5|Briefly described|p4, Fig. 2, p9-12|Neoproterozoic|Neoproterozoic|in Yeneena Basin,  top of Lamil Group. Appears to conformably overlie Puntapunta Formation, but contact not exposed. Mostly silicified sandstone; minor conglomerate, siltstone, and shale||||||
37330|Wilki Formation|62453|3|Fully described|p5 Fig. 3, 69|Cryogenian|Cryogenian|Of the Lamil Group. Geological Province: Paterson Orogen. Includes Kaliranu Member. Thickness: 1.4km. Conformably overlies Puntapunta Formation. Shale, siltstone, sandstone. ||||||
37330|Wilki Formation|64580|4|Described|map legend||Neoproterozoic|Of Lamil Group. Fine- to medium-grained quartz sandstone; minor shale, laminated sandstone, and dolomite.||||||15-DEC-08
37330|Wilki Formation|64777|5|Briefly described|p3 Fig.4 |Neoproterozoic|Neoproterozoic|||Of the Lamil Group|||Sandstone; minor conglomerate, siltstone and shale.|
37330|Wilki Formation|64941|5|Briefly described|p27|Tonian|Tonian|Yeneena Basin. Age: c. 960 Ma, maximum depositional age, SHRIMP U-Pb detrital zircon.|see comments|At top of Lamil Group.||Overlies Puntapunta Formation.||
37330|Wilki Formation|65454|4|Described|p7 Fig.3, p8, p9 Fig.4, p23, p30 Fig.A1b|Cryogenian|Cryogenian|Yeneena Basin. Of Lamil Group. Mature quartzitic sandstone composed of upward-coarsening fine to coarse sandstone couplets overlain by a finer-grained siliciclastic unit (Kaliranu Member). A basal magnetic high produces curvilinear anomalies north of Minyari; this implies that the prospective Lamil Group continues north under cover.||||||
37330|Wilki Formation|65725|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Lamil Group. Overlies Puntapunta Formation. Fine- to medium-grained quartz sandstone. Massive to bedded. Minor shale and laminated sandstone. Province:Yeneena Basin (Centralian Superbasin)||||||26-FEB-13
37330|Wilki Formation|65826|4|Described|p1, p13, p15.|Neoproterozoic|Neoproterozoic|Formerly Wilki Quartzite of Chin et al. (1982). Sedimentary structures are rarely preserved; a shallow-marine environment is tentatively inferred. Fractured and sheared sandstones may contain significant groundwater supplies.||Unit in Lamil Group.||Conformably overlies Puntapunta Formation. Is intruded by Mount Crofton Granite.|A monotonous sequence of silicified fine- to medium-grained sandstone, and minor recessive shale and laminated sandstone; the sandstone is moderately sorted, quartz-rich, sub-rounded to well rounded grains in a quartz-sericite matrix.|
37330|Wilki Formation|67202|4|Described|p7, p59, p62-63, p118, p128, p157, p183|Neoproterozoic|Neoproterozoic|See also p185, p189-190, p196, p198, p203, p281. Yeneena Basin. An aquifer supplying water to the Telfer mining community. Shallow-marine deposits c.1.4km thick. Gravity and aeromagmetic interpretation. Appears as Wilki Quartzite on p190.||Lamil Group.||Intrerpreted to conformably overlie the Puntapunta Formation.|A lower section of graphitic shale, siltstone and fine-grained silty sandstone, overlain by fine- to medium-grained sandstone with interbedded silty sandstone.|
37330|Wilki Formation|68902|5|Briefly described|p12, p15-18, p20, p25, p27|Neoproterozoic|Mesoproterozoic|Source of curvilinear positive magnetic anomalies. Up to 1.4 km thick. Forms resistant ridges between and around granite plutons.||Lamil Group|||Ferruginised sandstones and siltstones.|
37330|Wilki Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|Yeneena Basin.||Lamil Group.||||
37330|Wilki Formation|69590|4|Described|500k_geologyp08_lut.csv|Neoproterozoic|Neoproterozoic|Geological province: Paterson Orogen. Events: Musgrave Orogeny; Paterson Orogeny.||Unit of Lamil Group.|||Fine- to medium-grained quartz sandstone; minor shale, laminated sandstone, and dolomite|
37330|Wilki Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||quartzite, shale, siltstone, psammite|
37330|Wilki Formation|72034|5|Briefly described|500k_interpgeop16_lut|Ediacaran|Neoproterozoic|Yeneena Basin.||Lamil Group|||Fine- to medium-grained quartz sandstone; minor shale, laminated sandstone, and dolomite.|
37330|Wilki Formation|73345|6|Mentioned|p228|||Yeneena Basin[?].||||||
34562|Willespie Formation|12758|4|Described|p14, p3 Fig. 3|Late Permian|Late Permian|Of the Sue Group. Overlain Conformably overlain by Sabina Sandstone; conformably overlies the Redgate Coal Measures.||||||30-APR-13
34562|Willespie Formation|14227|5|Briefly described|Enclos. 2|Dorashamian|Kungurian|Topmost unit of the Sue Group. Overlies Redgate Coal Measures. Geol. Prov: Bunbury Trough, southern Perth Basin.||||||07-FEB-11
34562|Willespie Formation|22818|5|Briefly described|map|Late Permian|Late Permian|Sue Group||||||
34562|Willespie Formation|22819|5|Briefly described|map|Late Permian|Late Permian|Sue Group||||||
34562|Willespie Formation|22820|2|Defined|p8-9 Tbs. 1&2, p21|Late Permian|Late Permian|Of Sue Group. Contains unnamed seamlets. Conformable on Redgate C.M; unconformable below Leederville Fm. Max. thickness: >747m. Geol.prov: south Perth Basin. Numerous upward-fining cycles dominated by sandstone. Detailed lithology given.||||||12-AUG-08
34562|Willespie Formation|24443|5|Briefly described|Fig.31|Late Permian|Late Permian|Top unit of Sue Group. Conformably overlies Redgate Coal Measures. Conformably overlain by Sabina Sandstone. Geological Province: Perth Basin.||||||
34562|Willespie Formation|50107|5|Briefly described|Map legend|Permian|Permian|Of the Sue Group. Geological Province: Southern Perth Basin.||||||28-JUL-09
34562|Willespie Formation|60386|5|Briefly described|p296, 299, 312|Early Triassic|Guadalupian|Southern Perth Basin. Shown as Ufimian - Scythian. Non-marine.||||||
34562|Willespie Formation|67925|3|Fully described|ES p1-p4, Ch2 p10 fig 4, Ch2 p11, |Changhsingian|Kazanian|Deposited in complex lacustrine to meandering fluvial environments. Reservoir quality of this formation is poor with total porosity and effective porosity around 9.7% and 2% respectively. Permeability is also low, rarely exceeding 0.3mD. A type section in a drillhole is mentioned as being 1060m thick at a depth interval of 3800m to 4600m. Palynology discussed. See also Ch2 p14-p15, Ch2 p19, Ch2 p26-p28, Ch2 p30-p32, Ch2 p35, Ch2 p37, Ch2 p44-p45, Ch2 p49, Ch2 p51, Ch3 p2, Ch3 p6, Ch3 p8, Ch3 p15-p16, Ch3 p33-p52, Ch4 p2, Ch4 p5-p8, Ch4 p15, Ch4 p18, Ch4 p31, Ch8 p5, Ch8 p7, Ch8 p11.||Sue Group||Conformably overlies the Redgate Coal Measures. Conformably overlain by the Sabina Sandstone. Unconformably overlain by the Warnbro Group.|Poorly sorted feldspathic sandstone with subordinate conglomerate, siltstone, shale and sporadic coal.|
34562|Willespie Formation|69029|6|Mentioned|p332|Permian|Permian|Of Perth Basin.||||Overlain by Wagina Sandstone. Underlain by .||
34562|Willespie Formation|69081|5|Briefly described|p737 Fig.1|Lopingian|Lopingian|Presented as Willespie Fm in figure. Geol. Prov: Perth Basin.||Sue Group.||Is overlain by Sabina Sandstone; overlies Redgate Coal Measures.||23-JUL-15
34562|Willespie Formation|69182|6|Mentioned|Ch2 p9, Ch2 p45, Ch2 p47-p49|Late Permian|Late Permian|Perth Basin. See also Ch2 p55, Ch2 p57, Ch2 p60, Ch2 p64-p66, Ch2 p84, Ch2 p91, Ch2 p92, Ch2 p94-p96, Ch2 p98, Ch2 p100, Ch2 p102, Ch2 p104, Ch2 p106, Ch2 p108, Ch2 p110.||Sue Group||Overlies the Redgate Coal Measures. Unconformably overlain by the Sabina Sandstone.||
34562|Willespie Formation|69297|6|Mentioned|p175, p189|Changhsingian|Wordian|Vlaming Sub-basin, South Perth Basin. ||Sue Group||Overlies the Redgate Coal Measures. Overlain by the Sabina Sandstone.||
34562|Willespie Formation|70097|5|Briefly described|p2, p19 Fig.3|Wuchiapingian||Southern Perth Basin. Bunbury Trough.||Sue Group||Overlies Redgate Coal Measures. Is overlain by Sabina Sandstone.|Deglaciation, deltaic sediments. Sandstone.|12-SEP-17
34562|Willespie Formation|70099|5|Briefly described|Fig.4; p5|Wuchiapingian|Wordian|Southern Perth Basin. Correlated to seismic package Mentelle 1B, with Sabina and Lesueur Sandstones.||Sue Group.||Overlies Redgate Coal Measures. Is overlain by Sabina Sandstone.||
34562|Willespie Formation|70128|5|Briefly described|p449|Permian|Permian|Southern Perth Basin.||Sue Group.||Conformably overlies Redgate Coal Measures. Is overlain conformably by Sabina Sandstone.||
34562|Willespie Formation|70774|5|Briefly described|p5 fig 3|Dzhulfian|Kazanian|Southern Perth Basin.||||Unconformably? Overlies the Redgate Coal Measures.||
34562|Willespie Formation|71146|5|Briefly described|p6,  p43 fig 33|Lopingian|Guadalupian|Perth Basin.||||Overlies the Redgate Coal Measures. Overlain by the Sabina Sandstone.|Sandstone.|
34562|Willespie Formation|71377|5|Briefly described|p7, p77|Permian|Permian|Perth Basin. Some authors suggest an unconformable relationship with the Sabina Sandstone (Millar and Reeve, 2014; Mory et al, 2015).||Sue Group||Conformably overlain by the Sabina Sandstone.||
34562|Willespie Formation|71958|5|Briefly described|p34|Changhsingian|Wordian|Vlaming Sub-basin.||Sue Group||Overlies the Redgate Coal Measures. Overlain by the Sabina Sandstone.||
34562|Willespie Formation|72258|5|Briefly described|p129|Lopingian|Guadalupian|Of Perth Basin.||||Overlain by Sabina Sandstone. Underlain by Redgate Coal Measures. Laterally grades into Dongara Sandstone, Wagina Sandstone and Beekeeper Formation.||
74629|Willie Creek Calcarenite|64449|2|Defined|p75, p76, p79 Tb. 5, p111-113|Holocene|Holocene|Underlies Kennedys Cottage Limestone and Horsewater Soak Calcarenite mainly, but also Christine Point Clay and/or Sandfire Calcilutite. Underlain by Mowanjum Sand. Thickness: 5m. Age: 3060+/-600 yrs BP and 6910+/-180 yrs BP.||||||07-JUL-20
74629|Willie Creek Calcarenite|73213|6|Mentioned|958 Fig.3(b)|||||||Is overlain by Kennedys Cottage Limestone.||19-JAN-23
37494|Willy Willy Formation|50195|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Scorpion Group (Bangemall Supergroup).  Interbedded stromatolitic dolomite, siltstone and sandstone.  Geological Province: Scorpion Basin.||||||
37494|Willy Willy Formation|64580|4|Described|map legend||Mesoproterozoic|Of Scorpion Group. Interbedded stromatolitic dolomite and siltstone; minor sandstone.||||||15-DEC-08
37494|Willy Willy Formation|64772|5|Briefly described|p13, Plate 1  legend|Mesoproterozoic|Mesoproterozoic|Of the Scorpion Group. Interbedded stromatolitic dolomite and siltstone; minor sandstone.||||||01-MAR-11
37494|Willy Willy Formation|70795|4|Described|500k_interpgeop14_lut.csv|Mesoproterozoic|Mesoproterozoic||1620-1080 Ma||||Interbedded stromatolitic dolomite and siltstone; minor sandstone.|
37494|Willy Willy Formation|71158|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Scorpion Basin.||Scorpion Group.|||Interbedded stromatolitic dolomite, siltstone and sandstone; commonly contorted bedding. Section only.|
37494|Willy Willy Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||crystalline dolostone/dolomite, siltstone, sandstone|
37494|Willy Willy Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Paleoproterozoic|Scorpion Basin.||Scorpion Group|||Interbedded stromatolitic dolomite and siltstone; minor sandstone.|
27616|Wilson Cliffs Sandstone|7433|6|Mentioned|p25 Fig.2. |||Canning Basin.||||||
27616|Wilson Cliffs Sandstone|23212|4|Described|Table.1 p6||Early Ordovician|Facies equivalent of Nambeet Formation.||||||
27616|Wilson Cliffs Sandstone|33738|6|Mentioned|p55|||||||||
27616|Wilson Cliffs Sandstone|35119|4|Described|p452 Fig.3, p467|Arenig|Arenig|Name proposed for sandstones between 2847m and 3503 m in Wilson Cliffs No. 1 well. This is the type section. Incomplete sections at the base of McLarty No. 1 and Kidson No.1. Upper part equivalent to Gap Creek and Willara formations, lower part equivalent to Nambeet and Emanuel formations. Deposited in intertidal to subtidal environment. Scarce well-preserved macrofossils include trilobites, graptolites, bivalves, brachiopods.||||Overlain conformably [?] by Goldwyer Formation. Rests unconformably on ferruginous shale of Cambrian- Upper Proterozoic? age.|Variety of sandstones with subordinate siltstone, limestone and, in upper part, dolomite.|21-APR-17
27616|Wilson Cliffs Sandstone|37369|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
27616|Wilson Cliffs Sandstone|38878|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
27616|Wilson Cliffs Sandstone|40127|6|Mentioned|p9|||||||||
27616|Wilson Cliffs Sandstone|40136|5|Briefly described|p43|||||||||
27616|Wilson Cliffs Sandstone|41854|6|Mentioned|Fig.1|||||||||
27616|Wilson Cliffs Sandstone|43746|6|Mentioned|Fig.2,p11|Llanvirnian|Arenigian|||||||
27616|Wilson Cliffs Sandstone|44143|4|Described|p.426, p441 Table 4-19|Ordovician|Ordovician|Up to 656m thick; sandstone & dolomite; shallow marine. Passes laterally into Nambeet Formation. Type section between 2,847 and 3,503m in Wilson Cliffs 1 (WILSON: 22deg 16' 39" S, 126deg 46' 55" E). Contains trilobites, graptolites, bivalves, conodonts and microflora; Arenigian.||||||24-NOV-17
27616|Wilson Cliffs Sandstone|45158|3|Fully described|p28|||||||||
27616|Wilson Cliffs Sandstone|62794|6|Mentioned|p298|Early Ordovician|Early Ordovician|Canning Basin. Correlated with Horn Valley Siltstone, Amadeus Basin (Webby et al 1981).||||||
27616|Wilson Cliffs Sandstone|64334|5|Briefly described|p39-41, 43|Ordovician|Ordovician|Eastern Canning Basin; subsurface only. Tremadoc-Arenig.||||Is overlain unconformably by Goldwyer Formation.|Sandstone.|
27616|Wilson Cliffs Sandstone|64643|5|Briefly described|p3 Fig. 2|Middle Ordovician|Lower Ordovician|||||||
27616|Wilson Cliffs Sandstone|65301|5|Briefly described|p5 Fig. 4|Middle Ordovician|Early Ordovician|Geological province: Canning Basin.||||||
27616|Wilson Cliffs Sandstone|65449|5|Briefly described|p3, p6, p14; Plate 1|Middle Ordovician|Early Ordovician|Identified at the base of Kidson 1, Patience 2 and Wilson Cliffs 1.||||Lateral equivalent of Nambeet Formation.|Sandy and conglomeratic (near basin margin) facies.|08-APR-20
27616|Wilson Cliffs Sandstone|68007|3|Fully described|p1-2, p4-5, p12-15, Plates 1, 2|Middle Ordovician|Early Ordovician|Canning Basin. Type section is the interval 2847-3503m in Wilson Cliffs 1 stratigraphic well (McTavish and Legg, 1976). Marine sediments with common shelly fossils; conodonts. c.158.8m thick in Patience 2 well. Oil and gas shows. TOC data tabulated. Generally poor to very poor reservoir potential. Composite well log.||||Is overlain by Goldwyer Formation, probably disconformably. Equivalent to Nambeet Formation.|Pale grey, very fine- to fine- (rarely medium-) grained quartz sandstone with variable proportions of interbedded medium to dark grey siltstone.|24-FEB-20
27616|Wilson Cliffs Sandstone|68902|6|Mentioned|p9 fig 5|Ordovician|Ordovician |||||||
27616|Wilson Cliffs Sandstone|69182|6|Mentioned|Ch4 p9-p12, Ch4 p40-p41|Lower Ordovician|Lower Ordovician|Canning Basin. See also Ch4 p45, Ch4 p47, Ch4 p50-p58, Ch4 p74, Ch4 p79-p82, Ch4 p92, Ch4 p94.  ||||Unconformably overlain by the Goldwyer Formation.||
27616|Wilson Cliffs Sandstone|69883|6|Mentioned|p4, p22|Arenig|Tremadocian|Canning Basin. Conodont zones and supersequences provided. Intersected in Wilson Cliffs and Contention Heights 1. This unit is interpreted as an age equivalent of the Willara and Nambeet formations. Contact with the Goldwyer Formation is gradational in the Stratotype (Wilson Cliffs 1 -2847m).||||Conformably overlain by the Goldwyer Formation.||
27616|Wilson Cliffs Sandstone|70774|5|Briefly described|p4|Middle Ordovician|Early Ordovician|Willara and Kidson Sub-basins, Canning Basin.||||Unconformably? overlain by the Goldwyer and Willara Formations. Equivalent to the Nambeet Formation.||06-FEB-20
27616|Wilson Cliffs Sandstone|71146|5|Briefly described|p6, p24|Middle Ordovician|Early Ordovician|Canning Basin. Thickness exceeds 731m in Wilson Cliffs 1.||||Overlain by the Willara Formation.|Sandstone.|
27616|Wilson Cliffs Sandstone|71171|6|Mentioned|p1-p2, p4-p5, p18|||Canning Basin.||Prices Creek Group||Laterally equivalent to the Nambeet Formation.||
27616|Wilson Cliffs Sandstone|71592|5|Briefly described|Appendix A.|||Canning Basin.|561+/-4 Ma (MDA: U-Pb zircon SHRIMP)||||Quartz-rich coarse-grained sandstone.|
27616|Wilson Cliffs Sandstone|71870|5|Briefly described|p5|||Canning Basin.||||Equivalent to the Nambeet Formation.||
27616|Wilson Cliffs Sandstone|71894|5|Briefly described|p4|Lower Ordovician|Lower Ordovician|Canning Basin.|||||Sandstone.|
27616|Wilson Cliffs Sandstone|72499|5|Briefly described|p7 Fig.6.|Early Ordovician|Early Ordovician|Located in the Willara Sub-basin.||||Shown as unconformably underlying Goldwyer Formation and laterally equivalent to Nambeet Formation.||
27616|Wilson Cliffs Sandstone|73117|5|Briefly described|p3|Lower Ordovician|Lower Ordovician|Canning Basin. Lower boundary marked by a major unconformity[?] [related to the Samphire Marsh Movement?].||||Unconformably overlain by[?] Goldwyer Formation. Equivalent to Nambeet Formation.|Dominantly sandstone.|
27616|Wilson Cliffs Sandstone|73344|4|Described|p. 2-4, 6, 40, 50-51, 53, 56, 62-65,Pl.3|Early Ordovician|Early Ordovician|Canning Basin, far southeast. Known only from the subsurface. Defined by McTavish and Legg (1976). Type section from the Wilson Cliffs 1 exploration well between 2847-3503 m [656 m thickness]. Contains the P. elegans - Berg. extensus biozone. A distinct change from sandstone and sandy limestone to mudstone is identified at the top of the unit. Biostratigraphy suggests the unit may be unconformably overlain by either the Goldwyer Formation or Willara Formation.||||Unconformably overlain by Goldwyer Formation. Equivalent to Nambeet Formation (and members therein), and Emanuel Formation, Kudata Dolomite, and Kunian Sandstone of Prices Creek Group.|The upper portion is defined as a white, very fine- to fine-grained sandstone. The lower portion is red-brown and ferruginous with common medium to coarse grains. Both sections are tight and highly silicified with common quartz overgrowths.|
27616|Wilson Cliffs Sandstone|73345|6|Mentioned|p228, p230|||Detrital zircon geochronology from Wilson Cliffs 1 is similar to Fly Flat Member, Nambeet Formation.||||Equivalent to Fly Flat Member (Nambeet Formation).||
27616|Wilson Cliffs Sandstone|73346|6|Mentioned|p3, p25-27|Middle Ordovician|Early Ordovician|Canning Basin, southeast. Deposited in shallow marine environments.||||||
77786|Wilson Creek intrusion|60498|6|Mentioned|p1019-1020.|Paleoproterozoic|Paleoproterozoic|No lithology was stated for the stratigraphic name. Electron microprobe geochemical analyses of apatites are detailed.||||||
77786|Wilson Creek intrusion|71873|5|Briefly described|p426-430,433-434,437,439-440,444|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province. U-Pb detrital zircon magmatic age include 1847+\-3 and 1848+\-5 Ma.|||||Cumulates include melatroctolites to plagioclase peridotites with coarse cumulus olivine.|
33446|Wilson Well Gneiss|23416|5|Briefly described|Map Legend|Archean|Archean|Of Carlindi Granitoid Complex, Pilbara Craton.||||||07-NOV-08
33446|Wilson Well Gneiss|23755|5|Briefly described|p48|Archean|Archean|Age: >3480 Ma. See also page 18 Table 2.||||||07-NOV-08
33446|Wilson Well Gneiss|63420|5|Briefly described|Map legend|Archean|Archean|Of Tambina Supersuite.  Age: c.3420Ma. Geological Province: Pilbara Craton. Heterogeneous, migmatic tonalitic orthogneiss; minor schlieric hornblende granodiorite.||||||07-NOV-08
33446|Wilson Well Gneiss|63441|5|Briefly described|p7 Tb. 2|Archean|Archean|Of the Tambina Supersuite. Age: >c.3462Ma. Geological province: Pilbara Craton. (NOTE: Incorrectly placed in Callina Supersuite in table 2, p7).||||||07-FEB-11
33446|Wilson Well Gneiss|64936|6|Mentioned|bedrock geology figure|Archean|Archean|Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
33446|Wilson Well Gneiss|66217|5|Briefly described|p5, p28.|||East Pilbara Terrane, Pilbara Craton.||Unit in Tambina Supersuite.||Intrudes Pilbara Supergroup.|A heterogeneous unit of weakly migmatitic tonalite gneiss, medium-grained and foliated, with granoblastic texture, containing sparse enclaves of medium-grained quartz diorite; foliated.|
33446|Wilson Well Gneiss|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c. 3420 Ma|Of the Tambina Supersuite.||Enclaves of the Wilson Well Gneiss occur within the Kadgewarrina Monzogranite.|Heterogeneous migmatitic, tonalitic orthogneiss and schlieric hornblende granodiorite.|
33446|Wilson Well Gneiss|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. U-Pb SHRIMP age from Van Kranendonk (unpublished).|c.3420 Ma|Of the Tambina Supersuite.|||Heterogeneous, migmatitic, tonalitic orthogneiss; minor schlieric hornblende granodiorite.|
33446|Wilson Well Gneiss|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c. 3420 Ma|Of the Tambina Supersuite.|||Heterogeneous, migmatitic, tonalitic orthogneiss and schlieric hornblende granodiorite.|02-MAY-14
33446|Wilson Well Gneiss|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Tambina Supersuite|||Heterogeneous, migmatitic, tonalitic orthogneiss and schlieric hornblende granodiorite|
33446|Wilson Well Gneiss|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|3459-3410 Ma (inferred)|Unit of Tambina Supersuite.|||Heterogeneous, migmatitic, tonalitic orthogneiss and schlieric hornblende granodiorite|
33446|Wilson Well Gneiss|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||felsic gneiss, granodiorite|
33446|Wilson Well Gneiss|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|||Tambina Supersuite|||Heterogeneous tonalitic orthogneiss and schlieric hornblende granodiorite; migmatitic.|
30236|Wilthorpe Formation|7161|5|Briefly described|p96 Fig.6|||Less than 1500m thick (from p96 Fig.6).||||Overlain by the Robinson Range Formation. Underlain by the Labouchere Formation.|Submarine-fan, retrogradationally stacked, conglomerate-wedge parasequences.|
30236|Wilthorpe Formation|12099|4|Described|p676, p678 Fig.4, p682-3|Orosirian|Orosirian|Subdivided by Occhipinti et al. (1997).  Interpreted by Martin (1994) to be an upward-coarsening, deep-water turbidite complex derived from Yilgarn Craton material. Age from upper Wilthorpe Formation.|~2000 Ma.|Unit in Padbury Group.|Includes Heines and Beatty Park Members.|Overlain by Robinson Range Formation.||04-MAR-13
30236|Wilthorpe Formation|22694|5|Briefly described|p7|||||||||
30236|Wilthorpe Formation|22940|3|Fully described|p17, Fig.6 p14|Paleoproterozoic|Paleoproterozoic|Formerly 'Wilthorpe Conglomerate'. See also Table 2 p12, p10. Of Padbury Group.||||||07-NOV-08
30236|Wilthorpe Formation|23592|5|Briefly described|p12|Paleoproterozoic|Paleoproterozoic|Age: 1996+/-35 Ma (SHRIMPU-Pb zircon). Of Padbury Group. Geological Province: Padbury Basin.||||||07-NOV-08
30236|Wilthorpe Formation|23744|4|Described|p15|Paleoproterozoic|Paleoproterozoic|Formerly Wilthorpe Conglomerate. See also page 24. Of Padbury Group. Geological Province: Padbury Basin.||||||07-NOV-08
30236|Wilthorpe Formation|23747|5|Briefly described|p15|Paleoproterozoic|Paleoproterozoic|Of Padbury Group. Geological Province: Padbury Basin.||||||07-NOV-08
30236|Wilthorpe Formation|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Padbury Group. Geological Province: Padbury Basin||||||
30236|Wilthorpe Formation|23749|5|Briefly described|p13|Proterozoic|Proterozoic|Of Padbury Group. Geological Province: Padbury Basin.||||||
30236|Wilthorpe Formation|23750|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Padbury Group. Geological Province: Padbury Basin.||||||
30236|Wilthorpe Formation|23890|5|Briefly described|p21 Fig.11|||Of Padbury Group. Geological Province: Padbury Basin.||||||
30236|Wilthorpe Formation|24028|5|Briefly described|p296|Paleoproterozoic|Paleoproterozoic|Age: 1996+/-35Ma.||||||07-NOV-08
30236|Wilthorpe Formation|43830|5|Briefly described|Map Legend||Paleoproterozoic|Padbury Basin||||||07-NOV-08
30236|Wilthorpe Formation|43831|5|Briefly described|Map Legend||Paleoproterozoic|Padbury Basin||||||07-NOV-08
30236|Wilthorpe Formation|49896|1|Redefined|p57-58, p3 Tb. 2|Paleoproterozoic|Paleoproterozoic|Of Padbury Group. Includes Heins and Beatty Park Members. Overlies Labouchere Formation; unconformable on Narracoota and Ravelstone Formations. Unconformable beneath Bangemall Group. Max. age: 1996+/-35 Ga. Max. thickness: 1300m in type section.||||||07-NOV-08
30236|Wilthorpe Formation|50222|5|Briefly described|p320 Fig. 3, p327|Paleoproterozoic|Paleoproterozoic|Of the Padbury Group.  Contains the Beatty Park and Heines Members.  Overlain by Millidie and Robinson Range Formations.  Max. thickness: 1300m.  Geological Province: Padbury Basin.||||||07-NOV-08
30236|Wilthorpe Formation|62289|5|Briefly described|plate 1, p4 Fig. 2|Palaeoproterozoic|Palaeoproterozoic|Of Padbury Group; includes Heines Member. Geol. Prov: Padbury Basin.||||||
30236|Wilthorpe Formation|63866|5|Briefly described|p164|||Western Glengarry Basin.||Padbury Group||||
30236|Wilthorpe Formation|64580|4|Described|map legend||Paleoproterozoic|Of Padbury Group. Conglomerate; Quartz clasts and some chert, quartz wacke, and granitoid rock clasts; quartz wacke and finely bedded siltstone; locally chloritic; graded beds.||||||15-DEC-08
30236|Wilthorpe Formation|65408|5|Briefly described|p83.|Paleoproterozoic|Paleoproterozoic|||Unit in Padbury Group.|Includes Beatty Park and Heines Members.||Quartz-pebble conglomerate.|17-JAN-12
30236|Wilthorpe Formation|65411|5|Briefly described|p88, p90.|Paleoproterozoic|Paleoproterozoic|||Unit in Padbury Group.|Includes Heines and Beatty Park Members.|Conformably and gradationally overlies Labouchere Formation. Is conformably overlain by, and grades into, Robinson Range Formation.|Abundant quartz pebble conglomerate, polymictic conglomerate, mafic clastic rocks, siltstone.|
30236|Wilthorpe Formation|65419|1|Redefined|p37, p38, pp40-42.|Paleoproterozoic|Paleoproterozoic|Originally the Wilthorpe Conglomerate of Gee (1979, 1987); the Wilthorpe member of Windh (1992); later the Wilthorpe Formation of Martin (1994, in prep.). Redefined in this study to includes outcrops previously mapped as Labouchere Formation in the Mount Padbury and Mount Fraser areas; also includes Heines and Beatty Park Members that outcrop on Bryah and Padbury 1:100 000 sheets respectively. Lithology is also redefined, and hence the name is formally changed from Wilthorpe Conglomerate to Wilthorpe Formation.  Named after Wilthorpe mining centre; type section 4 km NE of there. 400 - 1300 m thick. U-Pb age from detrital zircons.|1996 +/- 35 Ma (max. deposition; Nelson, 1997).|Unit in Padbury Group.|Includes Beatty Park and Heines Members.|Conformably overlies Labouchere Formation. Is faulted against the Narracoota Formation. Is overlain conformably by the Robinson Range Formation.|Quartz and chert pebble conglomerate, quartz wacke, sericitic siltstone, chlorite-quartz shale, siltstone and wacke, polymictic conglomerate with carbonate matrix, quartz-sericite-hematite schist, dolomitic sandstone, finely laminated chert lenses.|
30236|Wilthorpe Formation|65896|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Padbury Group. Includes Beatty Park Member. Quartz pebble conglomerate including quartzite and some chert pebbles; quartz wacke and finely bedded siltstone; graded units; metamorphosed. ||||||
30236|Wilthorpe Formation|66112|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Padbury Group. Pebble to boulder conglomerate; clasts include vein quartz, minor chert, quartz wacke, and granitoid; quartz wacke and finely bedded siltstone; locally chloritic; graded beds; unnamed units of chert and finely-bedded siltstone.||||||
30236|Wilthorpe Formation|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic|||Padbury Group|Includes Beatty Park Member, Heines Member||Conglomerate; quartz clasts and some chert, quartz wacke, and granitoid rock clasts; quartz wacke and finely bedded siltstone; locally chloritic; graded beds|
30236|Wilthorpe Formation|69003|5|Briefly described|p16|||Padbury Basin, Capricorn Orogen. Deep-water turbidites.||Padbury Group.|Heines, Beatty Park Members.|Conformably overlies Labouchere Formation.Is overlain conformably by Robinson Range Formation.|Turbidites.|
30236|Wilthorpe Formation|69028|5|Briefly described|Map Legend|Orosirian|Orosirian|Padbury Basin.||Of the Padbury Group.||Overlies Labouchere Formation. Is overlain by Millidie Creek Formation.|Pebble to boulder conglomerate, clasts include vein quartz, minor chert, quartz wacke, and granitoid; quartz wacke and finely bedded siltstone, locally chloritic, graded beds.|06-MAY-14
30236|Wilthorpe Formation|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|||Padbury Group|Includes Beatty Park Member, Heines Member||Pebble to boulder conglomerate; clasts include vein quartz, minor chert, quartz wacke, and granitoid; quartz wacke and finely bedded siltstone; locally chloritic; graded beds|
30236|Wilthorpe Formation|69596|5|Briefly described|p10-11|||Padbury Basin.|||Heines, Beatty Park Members.||Upward-coarsening, deep-water turbidites.|
30236|Wilthorpe Formation|70795|5|Briefly described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, West Australian Craton, Padbury Formation|1983-1811 Ma||||Pebble to boulder conglomerate, quartz wacke,siltstone and chert.|
30236|Wilthorpe Formation|70796|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|Padbury Basin, Capricorn Orogen.|ca 19831811 Ma (inferred)|Padbury Group|||Pebble to boulder conglomerate; clasts include vein quartz, minor chert, quartz wacke, and granitoid; quartz wacke and finely bedded siltstone; locally chloritic; graded beds.|
30236|Wilthorpe Formation|70804|4|Described|p2-p3, p8, p18-p19||Orosirian|Age derived from Nelson (1997). Previously the Wilthorpe Conglomerate of Gee (1987). Martin (1994) measured the type section (approx. 1300m thick) along the Talbot Divide. At the type section this unit forms a prominent ridge. See also p24-p26, p42-p43, plate 1.|c. <2000 Ma|Padbury Group|Includes the Beatty Park Member and the Heines Member.|Conformably (gradationally) overlies the Labouchere Formation. Conformably overlain by the Robinson Range Formation.|Quartz and chert-pebble conglomerate, quartz wacke, sericitic siltstone, chlorite-quartz shale, quartz-sericite-hematite schist, dolomitic sandstone and finely laminated chert lenses.|
30236|Wilthorpe Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone, siltstone, chert|
30236|Wilthorpe Formation|71269|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Of Padbury Basin. Events: Capricorn Orogeny (1817-1772 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv.|1983-1811 Ma (inferred)|Unit of Padbury Group.|Includes Heines Member.||Pebble to boulder conglomerate; clasts include vein quartz, minor chert, quartz wacke, and granitoid; quartz wacke and finely bedded siltstone; locally chloritic; graded beds|
30236|Wilthorpe Formation|71484|4|Described|p123,125,129-130,134-138|Orosirian|Orosirian|Geological province: Of Padbury Basin. Interpreted maximum depositional age of 1996+\-35 Ma or 2014+\-22 Ma (p129, no references provided); overlapping with, or younger than c. 2000 Ma dolerites in the Narracoota Formation. Primary mineral constituents have been metamorphosed to quartz, sericite, and locally chlorite, forming quartz-sericite schists and chlorite-quartz schists. Forms a 5000m thick turbidite complex with the Labouchere Formation that outcrops in the W Padbury Basin (Martin, 1998).||Unit of Padbury Group.|Includes Beatty Park Member.|Overlain by Robinson Range Formation or Bertibubba Supersuite. Underlain by Labouchere Formation.|Quartz- and chert-pebble conglomerate, quartz wacke, siltstone, chlorite-quartz mudstone, and dolomitic sandstone.|30-AUG-19
30236|Wilthorpe Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Padbury Basin.||Padbury Group|||Pebble to boulder conglomerate; clasts include vein quartz, minor chert, quartz wacke, and granitoid; quartz wacke and finely bedded siltstone; locally chloritic; graded beds.|
26220|Wiluna Hardpan|23147|5|Briefly described|p139|||||||||
26220|Wiluna Hardpan|29770|2|Defined|p73|early Quaternary|late Tertiary|Late Tertiary to Early Quaternary||||||
26220|Wiluna Hardpan|37343|6|Mentioned|p43|||||||||
26220|Wiluna Hardpan|39087|6|Mentioned|p17|||||||||
26220|Wiluna Hardpan|50188|6|Mentioned|p18|||Of Bettany and Churchwand (1974).||||||14-JUL-04
26220|Wiluna Hardpan|61155|5|Briefly described|p16|Early Pliocene|Middle Miocene|Overlies Weelumurra beds; overlain by Kumina Conglomerate. Age: 14-~2Ma. Thickness: 10m. Geological Province: West Fortescue Valley.||||||25-MAY-06
26220|Wiluna Hardpan|64633|6|Mentioned|p44 Fig.31.|Tertiary|Tertiary|Occurs in the Leonora-Mertondale area.||||||
24111|Windaning Formation|22774|4|Described|p571, Fig.2 p573|||Age of unit 2808+/-5 Ma. Should be elevated to the status of Group||||||
24111|Windaning Formation|23135|5|Briefly described|p279 Fig.1|||||||||
24111|Windaning Formation|23148|5|Briefly described|p112 Table.2|||||||||
24111|Windaning Formation|24160|5|Briefly described|p112.|||Regionally extensive unit.||Unit in Luke Creek Group.|||Jaspilitic BIF interlayered with volcaniclastic sedimentary rocks, felsic tuff, and minor volcanic rocks.|
24111|Windaning Formation|42533|3|Fully described|p49|||Name reserved.||||||
24111|Windaning Formation|44149|5|Briefly described|p35 fig 2-30, p36-39, p40, p42 Fig.2-43|Archean|Archean|See also p43 Fig.2-44, p44 Fig.2-46, p45 Fig.2-48, p47, p57 Fig.2-71, p58 Fig.2-72, -73. Of Murchison Province|~3000 ma.|Luke Creek Group||Overlies Gabanintha Formation. Overlain by Quinns Basalt.|Regionally extensive jaspilitic BIF interlayered with volcaniclastic sediments, felsic tuff and minor volcanic rocks.|30-JAN-17
24111|Windaning Formation|64891|6|Mentioned|p36|||||||||07-FEB-11
24111|Windaning Formation|68561|5|Briefly described|GA_geochron.csv|Neoarchean|Neoarchean|Data migrated from OZCHRON1. Original comment: 'emplacement: 13 concordant analyses from 8 grains'|2703+/-10 Ma U/Pb SHRIMP|||||
40798|Windidda Member|50195|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Frere Formation (Tooloo Subgroup).  Geological Province: Earaheedy Basin.||||||07-NOV-08
40798|Windidda Member|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Of Frere Formation. Stromatolitic carbonate and siltstone, jasper, and peloidal jasper.||||||15-DEC-08
40798|Windidda Member|64772|4|Described|p11, Plate 1,  p10 Fig. 5|Paleoproterozoic|Paleoproterozoic|Formerly' Windidda Fm". Now of Frere Fm. Max.thickness: ~800m (est.) Geol.prov: Earaheedy Basin.  Carbonate lagoonal environment. See also p9, p12, p18 Fig.8, p19 Fig.9, p20-21 Fig.10, p44 Fig.30, p69 App.4, p75 App.4 Tb.4.3.||Of Frere Formation (Tooloo Subgroup, Earaheedy Group)||Is overlain by Chiall Formation (angular carbonate clasts breccia contact, interpreted as submarine hardground)|Sequence of carbonate and fine-grained clastic rocks, and consists of laminated or stromatolitic carbonate, interbedded with maroon or grey-green micaceous mudstone and shale with some intraclastic breccia beds and jaspilitic chert beds.|25-NOV-13
40798|Windidda Member|65264|5|Briefly described|p27, p44 Appdx. 1|Paleoproterozoic|Paleoproterozoic|Of the Frere Formation (Tooloo Subgroup).||||||07-FEB-11
40798|Windidda Member|65472|5|Briefly described|p1, p3 Fig.2|||Thickness: ~600 m. Earaheedy Basin. Presented as Windidda Formation on p5 Fig.4.||Tooloo Subgroup||Overlies Frere Formation.|iron-rich shale and carbonates|
40798|Windidda Member|65692|6|Mentioned|p56|||See also references to Windidda Formation (p9-10, p55-56).||Frere Formation.||||
40798|Windidda Member|66427|5|Briefly described|p43, p46 Fig.4, p47 Fig.5, p59-61, p65|||Here replaces Windidda Formation (see references to that unit: p43 Fig.2, p46 Fig.4, p54, p63, p73). c.600 m thick. Interpreted as carbonate bank and lagoonal environment synchronous with deposition of granular iron-formation.||Unit in Frere Formation.|||Consists of stromatolitic carbonate, shale, and siltstone, minor jasperoidal beds and minor granular iron-formation.|
40798|Windidda Member|68055|5|Briefly described|p77-78|Proterozoic|Proterozoic|Earaheedy Basin. Originally mapped as a separate Formation. Between 60 and 150m thick.||Frere Formation.|||Dominated by chemical sediments. Stromatolitic carbonate, shale and siltstone, minor jasperoidal beds and granular iron formation.|
40798|Windidda Member|69003|5|Briefly described|p13 Fig.17, p14 Fig.18|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin. c.600m thick.||Frere Formation.||Is overlain unconformably by Chiall Formation.|Stromatolitic carbonate rock.|
40798|Windidda Member|69152|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin||Frere Formation|||Stromatolitic carbonate and siltstone, jasper, and peloidal jasper.|07-AUG-15
40798|Windidda Member|69313|6|Mentioned|p22 Fig.4.2, p23, p25, p61, p101, p115|Paleoproterozoic|Paleoproterozoic|Stromatolitic. ||Frere Formation||Overlain by the Chiall Formation.||08-SEP-17
40798|Windidda Member|69596|6|Mentioned|p10|||Earaheedy Basin.||Frere Formation.||||
40798|Windidda Member|70153|5|Briefly described|100k_geologyp10_lut.csv|Paleoproterozoic|Paleoproterozoic|||Frere Formation|||Stromatolitic carbonate and siltstone, jasper, and peloidal jasper.|
40798|Windidda Member|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||crystalline carbonate, jasper, limestone, shale|
40798|Windidda Member|71270|4|Described|100k_geologyp10_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen. Of Earaheedy Basin. See 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.||Unit of Frere Formation.|||Stromatolitic carbonate and siltstone, jasper, and peloidal jasper|
40798|Windidda Member|71484|5|Briefly described|p131-132|||Originally described by Hall and Goode, 1978; Bunting, 1986; given member status by Jones et al., 2001 following studies that established the unit as a facies variant within the Frere Formation.||Unit of Frere Formation.|||Siltstone and microbial carbonate.|30-AUG-19
74875|Windimurra Igneous Complex|64891|5|Briefly described|p37 Fig. 2, p42-43, p50-51 Tb. 1|Archean|Archean|Of the Meeline Suite. Overlain by Kantie Murdanna Volcanics which this complex intrudes. Age: 2780Ma; max.age: 2813+/-3Ma. Geological province: Murchison Domain. Hosts a vanadium mine operation. Layered gabbro, anorthosite, etc - lithology included||||||07-FEB-11
74875|Windimurra Igneous Complex|66195|4|Described|p601, Fig.3, p602, 597, 598, p599 Fig.2|Neoarchean|Mesoarchean|Murchison Domain, Yilgarn Craton. See figure 4 for more detail.||In Meeline Suite.||?Intrudes Norie Group.|Largest exposed mafic-ultramafic layered intrusion in Australia, ~6 km thick, divided into ultramafic zone (~500 m thick), lower zone (~2 km thick), main zone (~4 km thick), upper zone. Predominantly gabbroic.|17-APR-19
74875|Windimurra Igneous Complex|67129|6|Mentioned|vi, p1, p18 Fig.19, p20, p51-61, p63-64|Archean|Archean|Northern Murchison Domain, Youanmi Terrane. Largest exposed single mafic-ultramafic intrusion in Australia: c.2500 km2 and 6km thick. Coeval with Norie Group eruptions. Hosts significant vanadium mineralisation. 3055 +/- 40 Ma (Lu-Hf isochron). Stratigraphic column.|c.2810 Ma.|Meeline Suite|||Gabbro, gabbronorite, leucogabbro, peridotite and anorthosite. Anorthosite drop stones, slump structures and channels visible.|07-SEP-17
74875|Windimurra Igneous Complex|68108|6|Mentioned|p651 Tb.4|Mesoarchean|Mesoarchean||ca. 2813 Ma|Of the Meeline Suite.||||
74875|Windimurra Igneous Complex|68109|6|Mentioned|p659|||Youanmi Terrane. ||||Contemporaneous with the Norie Group and Narndee Igneous Complex.|Large layered mafic-ultramafic igneous complex.|
74875|Windimurra Igneous Complex|68110|5|Briefly described|p673, p678|Mesoarchean|Mesoarchean|~ 70 km southeast of Cue. Contains no hydrous mineral phases; has relatively flat REE patterns.|c. 2810 Ma|Of the Meeline Suite.||||
74875|Windimurra Igneous Complex|68287|5|Briefly described|Map Legend|Archean|Archean|Metamorphosed. One unnamed sub unit shown as c. 2813 Ma, but basis for age is unclear.||Of the Meeline Suite.|Includes Corner Well Gabbro and 52 unnamed units||Metagabbro with metagranite sheets; porphyritic gabbro with dolerite; leucogabbronorite interlayered with magnetitite; modally layered gabbro interlayered with leucogabbronorite; modally layered olivine gabbro, interlayered with leucogabbronorite.|
74875|Windimurra Igneous Complex|68519|5|Briefly described|Map Legend|Mesoarchean||Murchison Domain, Youanmi Terrane, Yilgarn Craton. An unnamed unit in the lower zone of this Complex has an age of c.2813 Ma.||Of the Meeline Suite.|||Metagabbro, magnetitite, gabbro, serpentinite, dolerite, leucogabbro, gabbronorite, olivine norite, troctolite, pyroxenite; all metamorphosed.|
74875|Windimurra Igneous Complex|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane.  Coarse-grained metagabbro U-Pb zircon age: 2813 +/- 3 Ma as the magmatic crystallization age of the gabbro protolith. metagabbronorite yielded an imprecise U-Pb zircon date of 2802 +/- 19 Ma (GSWA 194749, Wingate et al., 2012). See geochron file 194747.1.pdf.||Meeline Suite|Includes Corner Well Gabbro, 5 general, 2 Upper zone, 4 Lower zone and an Ultramafic zone unnamed unit.||Magnetitite; Metagabbro; Amphibolite; Meta-anorthosite; Dunite; Leucocratic peridotite; Anorthosite; Pyroxene cumulate gabbro; Olivine gabbro; Gabbronorite; Melanocratic norite; leucogabbro and layered magnetitite; Gabbro; Troctolite; metadunite|
74875|Windimurra Igneous Complex|68698|5|Briefly described|p9, p18|||A vast intrusive igneous complex produced by a proposed plume event, and followed by mafic-ultramafic volcanism (eg Polelle Group).|c.2810 Ma.|||Is intruded by Mount Kenneth Suite.||
74875|Windimurra Igneous Complex|69014|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane. Contains roof, lower, and border zones. Contains 17 unnamed facies, mapped separately. See legend for detailed lithology.|c. 2813 Ma|Of the Meeline Suite.|||Roof zone: porphyritic gabbro with dolerite; metamorphosed. Lower zone: olivine gabbro, metamorphosed. Border zone: metagabbro.|30-APR-14
74875|Windimurra Igneous Complex|69404|6|Mentioned|p2|||Synchronously emplaced with the Narndee Igneous Complex and the Norie Group.|||||Mafic to ultramafic rocks.|
74875|Windimurra Igneous Complex|69583|4|Described|p20,p47-50,p54-57,p59,p67,p71-75,p79|Mesoarchean|Mesoarchean|See also p83-84, p87, p93-94, p97-111, p113, p115, p117, p119-121, p123, p149-150, p154, p168, p173, p175-177; Plate 2. Eastern Murchison Domain. The type example of the Meeline Suite. Derived from a different parent magma from that of the Boodanoo Suite (Narndee Igneous Complex). Voluminous: 2500 km2, and perhaps 6km thick. Has an overall funnel-shaped form comprising two lobes (E and W). Surprisingly, this unit does not provide an expression in the MT Line 10GA-YU1. Near-surface zones have high conductivity. Mineralisation style, geochronological data, igneous stratigraphic column detailed. Defined well by gravity field worms; forward modelling, seismic interpretation detailed.|2813 +/- 3 Ma (Wingate et al., 2012).|Meeline Suite.|Corner Well Gabbro.|Is overlain by Kantie Murdana Volcanics Member. Is sheared against and intrudes Norie Group.|Mafic and ultramafic rocks: metagabbro and metaleucogabbro, locally with abundant metagranite. Hosts significant vanadium mineralisation in magnetitite layers.|
74875|Windimurra Igneous Complex|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean|||Meeline Suite||||
74875|Windimurra Igneous Complex|69586|5|Briefly described|p7, p19, p22|Mesoarchean|Mesoarchean|||Meeline Suite.||||
74875|Windimurra Igneous Complex|69617|6|Mentioned|p154|||Murchison Domain, Youanmi Terrane.|c.2800 Ma.|||||
74875|Windimurra Igneous Complex|69626|5|Briefly described|map legend|Archean|Archean|Informal Upper zone, Lower zone and Ultramafic zone contain multiple unnamed units. Additional unnamed units are also listed. Detailed lithology in legend. Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Meeline Suite|Corner Well Gabbro||Metagabbro (metagranite lenses). Upper zone: interlayered metagabbro-metagabbronorite-layered magnetitite. Lower zone: interlayered olivine gabbro-leucogabbronorite. Ultramafic zone: interlayered metadunite-gabbro-anorthosite; Corner Well Gabbro.|
74875|Windimurra Igneous Complex|70140|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Comprises 10 un-named facies mapped separately, but grouped into Border, Lower and Upper zones.|2813 Ma.|Meeline Suite.|||Border zone: metagabbro, dolerite. Lower zone: gabbro, gabbronorite, leucogabbro, anorthosite. Upper zone: magnetite-rich gabbro, leucotroctolite, layered magnetitite, gabbronorite. All metamorphosed.|
74875|Windimurra Igneous Complex|70332|5|Briefly described|p76-84|Archean|Archean|Central Youanmi Terrane, Yilgarn Craton. Extends 78 x 42 km. No evidence for contamination had been reported. Appears as WIC after first one or two mentions in text.|2813 +/- 3 Ma (SIMS U-Pb; Wingate et al., 2012).||||Large layered mafic-ultramafic intrusion; notably lacking a primary hydrous phase. Large parts metamorphosed to greenschist or lower amphibolite facies.|
74875|Windimurra Igneous Complex|70419|4|Described|p1-26|Mesoarchean|Mesoarchean|Youanmi Terrane, Yilgarn Craton. A giant (~2500 km2) layered mafic-ultramafic intrusion; at a cumulative 11 km thick, it is the thickest identified globally. Referred to as WIC throughout. A potential target for Ni-Cr-PGE mineralisation. Is dissected by large shear zones and smaller faults. Consists of two lobes (separated by a discordant zone) comprising eight zones (e.g. ultramafic, lower, middle, upper, roof). Seismic and 3D model interpretations.|2813 Ma (Ivanic et al., 2010).|Meeline Suite.|Corner Well Gabbro.|Intrudes Norie Group. Is overlain by and intrudes the Kantie Murdana Volcanics Member and Mount Kenneth Suite.|Ultramafic cumulates, gabbro, dolerite, magnetitite, anorthosite.|
74875|Windimurra Igneous Complex|70420|6|Mentioned|p9 Fig.6|Archean|Archean|||||||
74875|Windimurra Igneous Complex|70770|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Two zones are mapped separately.|c.2813 Ma.|Meeline Suite.|||Metagabbro and metaleucogabbro, grades into metagabbronorite, locally schistose and sheared, with abundant metagranite, aplite and granophyre intrusive sheets. Magnetitite layers <1m thick in magnetite-rich gabbro; metamorphosed.|
74875|Windimurra Igneous Complex|70796|5|Briefly described|100k_interpgeol_lut.csv,|Mesoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 194747.1.pdf, 194749.1.pdf, Bungar100_2539_stratig.pdf, Coolamaninu100_2540_stratig.pdf, Windimurra100_2641_stratig.pdf, Wynyangoo100_2542_stratig.pdf, Youanmi100_2640_stratig.pdf. Numerous additional lithologies are provided.|ca 2813 Ma (inferred)||||Chromitite, serpentised peridotite, leucotroctolite, pyroxene rich gabbro, anorthosite, pyroxenite, serpentinite, lherzolite and dolerite.|
74875|Windimurra Igneous Complex|70830|5|Briefly described|p2-p5, p26-p28|||Hosts significant vanadium mineralization in magnetite layers. See also p29, p30-p33, p49-p53, p55.|2813+/-3 Ma|Meeline Suite||||
74875|Windimurra Igneous Complex|71159|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Eleven facies associations are mapped separately and grouped into three zones: Border zone, Lower zone and Roof zone.||Meeline Suite.|||Dolerite, gabbro, pyroxene peridotite, pyroxenite, olivine gabbronorite, leucotroctolite, leucogabbro, anorthosite, pegmatitic gabbro, porphyritic gabbro, chromite-bearing dunite interlayered with gabbro and anorthosite; all metamorphosed.|
74875|Windimurra Igneous Complex|71168|4|Described|p7-p8, p18, p21-p22, p59-p60|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Has a true thickness of approximately 6km and covers an area of 2500km^2.|c. 2813 Ma|Meeline Suite||Overlain by the Kantie Murdana Volcanics Member.||
74875|Windimurra Igneous Complex|71311|6|Mentioned|p794|||Northern Youanmi Terrane, Yilgarn Craton.||||||
74875|Windimurra Igneous Complex|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Youanmi Terrane. 8 informal subdivisions shown: roof zone, upper zone, middle zone, lower zone, ultramafic zone, border zone, and 2 other subdivisions. See detailed descriptions in source reference. Magnetitite; gabbro, leucogabbro. Porphyritic gabbro, dolerite. Leucogabbronorite, interlayered magnetitite. Gabbro/leucogabbro; gabbronorite, leucogabbronorite, minor pyroxenite. Olivine gabbro, grading into olivine gabbronorite; leucogabbronorite, pyroxenite. All metamorphosed. Metadunite; meta-gabbro, anorthosite; metaperidotite. Metagabbro; meta-dolerite. Metagabbro, metaleucogabbro; metagabbronorite;  w metagranite, aplite, and granophyre intrusive sheets.||Windimurra Igneous Complex||Includes Corner Well Gabbro and 10 unnamed units.|Magnetitite, gabbro, leucogabbro, dolerite, leucogabbronorite; interlayered. Gabbronorite, pyroxenite, olivine gabbro, olivine gabbronorite. All metamorphosed. Metadunite, anorthosite, metaperidotite; metagranite, aplite, granophyre intrusive sheets|
74875|Windimurra Igneous Complex|72491|6|Mentioned|p5 Fig.4, p7, 55|||Murchison Terrane, Yilgarn Craton. On p55 it is referred to as ""the Windimurra and Lady Alma mafic-ultramafic igneous complexes"". High-grade hornfelses were produced in their aureoles at 2825-2815 Ma. Appears as Windimura IC in Fig.4, and abbreviated to Windimurra complex on p7.||||||
74875|Windimurra Igneous Complex|73596|6|Mentioned|p1161|Mesoarchean|Mesoarchean|Kalgoorlie Terrane.|2813 +/- 3 Ma.|||||
30320|Windoo Sandstone|23621|2|Defined|p57 Appendix|Late Cambrian|Late Cambrian|Replaces parts of Gardiner beds.  See also page 36, 9 table 1. Type section included. Underlying unit Antrim Plateau Volcanics. Max. thickness 50 m.||||||06-DEC-06
30320|Windoo Sandstone|23622|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Ord Basin.||||||
30320|Windoo Sandstone|43302|5|Briefly described|Map Legend||Paleozoic|||||||07-NOV-08
30320|Windoo Sandstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Cambrian||Grouped as Cambrian-Ordovician sedimentary rock, Southern Bonaparte Basin|||||Quartz sandstone, minor mudstone, dolomite, stromatolitic chert.|04-AUG-15
30320|Windoo Sandstone|69634|4|Described|100k_interpgeop_lut.csv|Ordovician|Series 3|Geological province: Halls Creek Orogen. Of Southern Bonaparte Basin. Events: Alice Springs Orogen; Mount Eclipse Movement; Pertnjara-Brewer Movements.|509-443.4 Ma (Inferred)||||Quartz sandstone, minor mudstone, dolomite, stromatolitic chert|
30320|Windoo Sandstone|70154|5|Briefly described|100k_interpgeop_lut.csv||||||||Quartz sandstone; minor mudstone, dolomite and stromatolitic chert.|
30320|Windoo Sandstone|70826|6|Mentioned|p7 tbl 3|Ordovician|Cambrian|Ord Basin.||||||
30320|Windoo Sandstone|71267|4|Described|GEOL_LUT_CSV files|Early Ordovician|Series 2|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny (450-295 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma); King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|510-470 Ma (inferred)||||Quartz sandstone, minor mudstone, dolomite, stromatolitic chert|
40890|Windplain Group|24535|4|Described|p22, 23|Paleoproterozoic|Paleoproterozoic|Sedimentary. Overlain by Mooloogool Group. Unconformably overlies Archaean basement. Consisists of sandstone, shale, carbonate and evaporitic rocks indicating shallow epicontinental seas. Geological Province: Yerrida Basin.|||Includes Juderina and Johnson Cairn Formations.|||26-NOV-13
40890|Windplain Group|50222|4|Described|p321, p319 Fig. 2|Paleoproterozoic|Paleoproterozoic|Supersedes Windplain Subgroup.  Comprises siliclastic rocks, stromatolitic carbonate and evaporitic rocks overlain by shales.  Underlies Mooloogool Group.  Age: ca.2.17Ga.  Geological Province: Yerrida Basin.  See also p315 and p332.||||||07-NOV-08
40890|Windplain Group|50223|5|Briefly described|p349|Paleoproterozoic|Paleoproterozoic|Age: 2200Ma and 2173+/-64Ma (Woodhead and Hergt, 1997).  Geological Province: Yerrida Basin.||||||01-MAR-10
40890|Windplain Group|50226|5|Briefly described|p420|Paleoproterozoic|Paleoproterozoic|Siliclastic and evaporite sedimentary rocks, shale.  Unconformably overlain by the Yelma Formation (Earaheedy Group). Age: ca. 2.17 Ga.  Geological Province: Yerrida Basin.||||||07-NOV-08
40890|Windplain Group|63866|5|Briefly described|p152, p175|||Yerrida Basin.||||||
40890|Windplain Group|64580|6|Mentioned|map legend|||||||||
40890|Windplain Group|64725|6|Mentioned|p73.|Paleoproterozoic|Paleoproterozoic|Yerrida Basin.||||Is overlain unconformably by Yelma Formation.||
40890|Windplain Group|64772|5|Briefly described|p8, Plate 1 legend, p19 Fig. 9|Paleoproterozoic|Paleoproterozoic|Geological province: Yerrida Basin. Siliciclastics and and evaporites.||||||07-FEB-11
40890|Windplain Group|65472|6|Mentioned|p1, p2, p3 Fig.2, p8 Fig.7|||Yerrida Basin.|||Includes Juderina Formation, Johnson Cairn Formation.|Overlain by Mooloogool Group (contact poorly defined, but where exposed is discomformable); constituent (Juderina Formation) is unconformably overlain by outliers of Earaheedy Group.||24-SEP-15
40890|Windplain Group|65550|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Yerrida Basin. Includes Juderina Formation and its constituent, Finlayson Member.||||||18-AUG-10
40890|Windplain Group|68471|6|Mentioned|p17|||Yerrida Basin sag phase.|c.2.2-2.1 Ga.|||||
40890|Windplain Group|68561|5|Briefly described|GEOL_LUT_CSV folder + GEOCHRON files||Paleoproterozoic|Yerrida Basin, Capricorn Orogen|||Includes Juderina Formation, Johnson Cairn Formation.|||
40890|Windplain Group|69003|4|Described|p4, p10-13|||Yerrida Basin, Capricorn Orogen. Separated from the overlying unit by a 300-400 m.y. hiatus. Coastal and shallow-marine, grading to intertidal and supratidal and sabkha lagoon, deposits. Most sediments were sourced from the Yilgarn Craton.|||Juderina, Johnson Cairn Formations.|Is overlain disconformably by Mooloogool Group.|Siliciclastic rocks, stromatolitic carbonates, evaporites, and a thick sequence of shales.|
40890|Windplain Group|69152|5|Briefly described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin [??]|||Includes Juderina Formation, Johnson Cairn Formation.|||24-SEP-15
40890|Windplain Group|69166|6|Mentioned|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||Includes Johnson Cairn Formation, Juderina Formation|||
40890|Windplain Group|69583|5|Briefly described|Plate 2|Proterozoic|Proterozoic|Yerrida Basin.|||Johnson Cairn, Juderina Formations.|||
40890|Windplain Group|69596|5|Briefly described|p4, p9-10, p32-34, p36 Fig.27b, p37|Paleoproterozoic|Paleoproterozoic|Yerrida Basin, Capricorn Orogen. The disconformity at the top represents a c.330 m.y. hiatus. Conductivity discussed. Over 1020m thick in THD001 drillhole.|c.2170 Ma.||Juderina, Johnson Cairn Formations.|Is overlain disconformably by Mooloogool Group.|A succession of graphitic shales, carbonaceous siltstones and sandstones, stromatolitic dolomites, and mafic rocks.|
40890|Windplain Group|70136|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Yerrida Basin.|||Johnson Cairn Formation.|||
40890|Windplain Group|70153|5|Briefly described|100k_geologyp10_lut.csv|Paleoproterozoic|Paleoproterozoic||||Includes Johnson Cairn Formation, Juderina Formation.|||
40890|Windplain Group|70795|6|Mentioned|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 2_5m_interpgeop15_lut.csv, West Australian Craton|2500-1600 Ma||Includes Johnson Cairn Formation||Sandstone, siltstone, shale and chert breccia.|
40890|Windplain Group|70796|4|Described|2_5m_interpgeop15_lut.csv|Paleoproterozoic|Paleoproterozoic|Of the Yerrida Basin, Capricorn Orogen. See also 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv,  500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, Tieraco100_2545_stratig.pdg.|ca 2170 1600 Ma (inferred)||Includes the Johnson Cairn Formation and the Juderina Formation.||Sandstone, siltstone, shale, chert breccia|
40890|Windplain Group|70814|6|Mentioned|p48|||||||||
40890|Windplain Group|70826|6|Mentioned|p6 tbl 2, p9|Paleoproterozoic|Paleoproterozoic|Yerrida Basin over the Yilgarn Craton.|c. 2170 Ma|||Overlain by the Mooloogool Group.||21-APR-20
40890|Windplain Group|71269|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen, West Australian Craton. Of Yerrida Basin. Events: Capricorn Orogeny (1817-1772 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv, glengarry_100k_geologyp_lut.csv.|2170-1600 Ma (inferred)||Includes Johnson Cairn Formation, Juderina Formation.||Sandstone, siltstone, shale, chert breccia|
40890|Windplain Group|71270|5|Briefly described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen. Of Yerrida Basin. Events: Capricorn Orogeny (1817 - 1772 Ma). See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 100k_geologysub10_lut.csv, 2_5m_interpgeop15_lut.csv.|2170-1600 Ma (inferred)||Includes Johnson Cairn Formation, Juderina Formation.|||
40890|Windplain Group|71468|6|Mentioned|p24|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen, Yilgarn Craton. Of Yerrida Basin.||||||
40890|Windplain Group|71484|4|Described|p122-125,128-130,133-134,139|Orosirian|Rhyacian|Geological province: Of Yerrida Basin. Underlain by Archean Yilgarn basement rocks to the south and west. Faulted against, and unconformably on the Marymia Inlier (Paleoproterozoic reworked Yilgarn basement) to the NE.|2200-1990 Ma||Includes Juderina and Johnson Cairn formations.|Overlain by Mooloogool group/Killara Formation.|Siliclastic, carbonate, chert, chert breccia, volcaniclastic and, locally, mafic volcanic rock.|30-AUG-19
40890|Windplain Group|72034|6|Mentioned|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Johnson Cairn Formation, Juderina Formation.|||
40890|Windplain Group|72389|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Yerrida Basin. Gabanintha 1:100k map sheet 2644.|||Includes the Juderina Formation.|||28-AUG-20
24577|Winemaya Quartzite|24160|6|Mentioned|p26, p27 Tb.14|Proterozoic|Proterozoic|||Coomberdale Subgroup||||
24577|Winemaya Quartzite|24410|5|Briefly described|p139|Proterozoic|Proterozoic|Of the Coomberdale Subgroup (Moora Group). See also p142 Tb. 60.||||||24-NOV-09
24577|Winemaya Quartzite|36293|2|Defined|p69|Proterozoic|Proterozoic|||||||
24577|Winemaya Quartzite|36872|3|Fully described|p77|||||||||
24577|Winemaya Quartzite|37460|6|Mentioned|p178|||||||||
24577|Winemaya Quartzite|40347|6|Mentioned|p20|||||||||
24577|Winemaya Quartzite|40348|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Middle or Late||||||
24577|Winemaya Quartzite|40349|5|Briefly described|p14|||||||||
27255|Winifred Formation|7433|5|Briefly described|p33, p53.|Sakmarian|Sakmarian|||Unit in Grant Group.|||Fine-grained sandstone and siltstone, interpreted as varves; minor coal, fossiliferous limestone.|
27255|Winifred Formation|22718|6|Mentioned|P5|||||||||
27255|Winifred Formation|22738|5|Briefly described|12|Early Permian|Early Permian|Parent Grant Group. Overlying unit Carolyn Formation, underlying unit Betty Formation.||||||24-NOV-08
27255|Winifred Formation|22741|5|Briefly described|P25, Table3 P14||Permian|||||||
27255|Winifred Formation|22753|6|Mentioned|p535|||Obsolete subdivision of Grant Group||||||
27255|Winifred Formation|22765|6|Mentioned|P9||Permian|||||||
27255|Winifred Formation|22767|5|Briefly described|Table3 P16, P21||Early Permian|||||||
27255|Winifred Formation|22776|4|Described|Table.3|Early Permian|Early Permian|Fossil assemblage includes palynomorphs. Parent: Grant Group.||||||24-NOV-08
27255|Winifred Formation|23212|5|Briefly described|Table.1 p7||Early Permian|of Grant Group.||||||
27255|Winifred Formation|23765|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
27255|Winifred Formation|23766|4|Described|p14 Tb. 2|Early Permian|Late Carboniferous|Parent: Grant Group.   Thickness: 171m.  See also p18.||||||
27255|Winifred Formation|36224|5|Briefly described|Map legend|Early Permian|Early Permian|Shale, carbonaceous, pyritic; minor siltstone, fine sandstone.  Correct spelling of the name Winnifred Formation.||||||01-FEB-05
27255|Winifred Formation|36225|6|Mentioned|Map legend|Early Permian|Early Permian|Correct spelling of the name Winnifred Formation.||||||
27255|Winifred Formation|36634|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27255|Winifred Formation|37914|5|Briefly described|p450|||See also P449.||||||
27255|Winifred Formation|41215|6|Mentioned|p280|||See also P281||||||
27255|Winifred Formation|41315|6|Mentioned|p135|||||||||
27255|Winifred Formation|41839|4|Described|p26|||||||||
27255|Winifred Formation|42547|4|Described|p97|||Part of Grant Group.||||||
27255|Winifred Formation|42613|2|Defined|p6|Sakmarian|Sakmarian|Of Grant Group.||||||24-NOV-08
27255|Winifred Formation|43015|5|Briefly described|Table 1,p319|||Of Grant Group.||||||24-NOV-08
27255|Winifred Formation|43563|6|Mentioned|Fig.9,p15||Early Permian|||||||
27255|Winifred Formation|43816|6|Mentioned|p88|||||||||
27255|Winifred Formation|44143|4|Described|p.436 Table 4-19; p.446|Permian|Permian|Unit in Grant Group. Up to 300m thick; siltstone; possible deep marine or lagoonal. Interglacial deposits: conformably overlies Betty Formation; is overlain conformably by Carolyn Formation. Type section in TABLETOP (22deg 52' 40" S, 123deg 36' 20" E). Contains crinoids and bryozoans, microflora; Sakmarian.||||||24-NOV-17
27255|Winifred Formation|45158|4|Described|p22|||||||||
27255|Winifred Formation|49644|5|Briefly described|Table|||||||||
27255|Winifred Formation|61021|5|Briefly described|p37|Early Permian|Early Permian|Of the Grant Group. Shales. Geological Province: Canning Basin.||||||17-DEC-07
27255|Winifred Formation|64580|6|Mentioned|map legend|||Of Grant Group.||||||15-DEC-08
27255|Winifred Formation|64630|5|Briefly described|p31 Fig.2, p35|Sakmarian|Asseliean|Part of Grant Group. N.B. Tentative ages, awaiting further palynology work. Province: in Fitzroy Trough area of Canning Basin, underlies Carolyn Formation, overlies Reeves Formation. Palynology age: P. confluens.||||||24-NOV-09
27255|Winifred Formation|64643|5|Briefly described|p8|Sakmarian|Sakmarian|Of Grant Group in Fitzroy Trough. Does not crop out.||||||
27255|Winifred Formation|64971|5|Briefly described|p685 Fig. 2|Early Permian|Early Permian|||||||09-FEB-10
27255|Winifred Formation|64974|5|Briefly described|p148 Fig. 6|Sakmarian|Asselian|Of Grant Group. Geological Province: Canning Basin.||||||24-JUN-09
27255|Winifred Formation|64981|5|Briefly described|p669 Fig.3.|Sakmarian|Sakmarian|||Unit in Grant Group.||Overlies Betty Formation. Is overlain by Carolyn Formation.|Mainly non-marine shales.|
27255|Winifred Formation|64982|5|Briefly described|pp699-700.|||||Unit in Grant Group.|||Dominantly siltstone.|
27255|Winifred Formation|66949|4|Described|p10, p13, p17-18, p28; p52-54 Appx.2|Sakmarian|Sakmarian|See also p57 Appx.3, p60-65 Appx.4; p66-67,71-74,76-94 Appx.5; Plates 2-12. Type section detailed but in isolated outcrop; relationship to other units uncertain. Had been attributed to Cuncudgerie Sandstone by Veevers and Wells (1961). Up to 278m thick (in The Sisters 1); glacial posssibly lagoonal to lacustrine deposits. Contains crinoids, bryozoans, palynomorphs. Forms a sealing horizon in the Sundown and West Terrace fields on the Lennard Shelf. Available core and Formation picks detailed.||Unit in Grant Group.||Conformably overlies Betty Formation.|Siltstone, minor limestone; local sandstone units.|30-OCT-15
27255|Winifred Formation|68007|4|Described|p2, p9, p12, Plates 1, 2|Permian|Permian|Southern Canning Basin. c.41.5m thick in Patience 2 well. Composite well log. Two possible intervals might be assigned to this unit. The most likely is 822.5- 864 m.||Grant Group.||Overlies Betty Formation. Is overlain by Carolyn Formation. Equivalent to Calytrix Formation.|Dark grey, non-calcareous claystone, with minor carbonaceous specks; medium to light grey siltstone, argillaceous and arenaceous in part, occasionally calcareous and pyritic, with common carbonaceous specks.|20-FEB-20
27255|Winifred Formation|68656|6|Mentioned|GEOL_LUT_CSV/500k_geologyp08_lut|||||Grant Group||||
27255|Winifred Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Cisuralian|Pennsylvanian|||||||
27255|Winifred Formation|69182|5|Briefly described|Ch4 p84, Ch4 p88-90|||Canning Basin. Seals the underlying Reeves and Anderson Formations. ||Grant Group||Overlies the Reeves Formation.|Shale and siltstone.|
27255|Winifred Formation|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Grant Group.||||
27255|Winifred Formation|69693|5|Briefly described|p3-5, 7, 9-10|Sakmarian|Sakmarian|Lennard Shelf, Canning Basin. See also references to Winifred formation (p2, 4, 6).||||Overlies Betty Formation. Is overlain by Carolyn Formation. Equivalent to Calytrix Formation.|Mudstone.|
27255|Winifred Formation|72496|4|Described|p217-220, p222-225, p228, p230-231|Sakmarian|Sakmarian|Canning Basin, Lennard Shelf and Fitzroy Trough. Type section occurs in the southern-most part of the Canning Basin and there contains evidence of direct glacial sedimentation. Maximum thickness of 81m in Nerrima-1 well. Deposited in a shallow marine to lagoonal environment.||Grant Group||Equivalent to the Calytrix Formation. Overlies the Betty Formation. Overlain by the Carolyn Formation.||18-MAR-20
27255|Winifred Formation|72497|5|Briefly described|p4, p10.|Permian|Late Carboniferous|After Crowe and Towner, 1976. Upper part implied to be equivalent to Hoya Formation.||Grant Group||Shown as overlying Betty Formation and underlying Carolyn Formation.||
27255|Winifred Formation|72499|4|Described|p54 Fig.48, p93.|Cisuralian|Cisuralian|Associated facies recorded on well logs Sundown 1 and Sundown 3/3H (Lennard Shelf), The Sisters 1 and Scarpia 1 (Fitzroy Trough), Frome Rocks 2 (Jurgurra Terrace), Dampier Downs 1 and Roebuck Bay 1 (Broome Platform) and Perindi 1 (Pender Terrace).||Grant Group||Overlies Betty Formation and underlies Carolyn Formation.||
27255|Winifred Formation|73117|4|Described|[See comments].|||Of Crowe and Towner (1976). [Written as 'Winifred Formation' and 'Winifred' ... Formations]. Part of the 'three ladies' naming scheme proposed as a subdivision of the Grant Group. Authors consider this an informal unit. This scheme for constituents of the Grant Group has been widely applied but is considered flawed by the authors because of spatially isolated type sections. This unit has a particularly problematic type section. In its type area, it probably represents a shaly interval close to the top of the group. Informally called the 'middle shale' but appears to have a highly variable stratigraphic level within the group; thus, unlikely to represent coeval facies. p: 21-23, 25, 109, 114, 122, 125, 127, 130, 136, 139.||Grant Group|||Includes shale.|
30155|Winnama Formation|22754|5|Briefly described|p10|||Formerly the Olympio Formation (Dow and Gemuts, 1969) - renamed by Tyler et al (1997b).  Overlain unconformably by Red Rock Formation.||||||
30155|Winnama Formation|24173|6|Mentioned|p15, p18|||Possible correlative of parts of Halls Creek Group.||||||06-APR-05
30155|Winnama Formation|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Lamboo Complex.  Low- to medium-grade, metamorphosed sandstone, siltstone, mudstone, basalt, dolerite and carbonate.||||||07-NOV-08
30155|Winnama Formation|43855|5|Briefly described|Map Legend||Proterozoic|||||||
30155|Winnama Formation|44868|5|Briefly described|Map Legend||Proterozoic|||||||
30155|Winnama Formation|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Low- to medium-grade, metamorphosed sandstone, siltstone, mudstone, basalt, dolerite, and carbonate.||||||15-DEC-08
30155|Winnama Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.|||Includes unnamed member.||Lithic metasandstone, metasiltstone, metamudstone, metabasalt, metadolerite, and metacarbonate; low to medium grade.|04-AUG-15
30155|Winnama Formation|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv. |||||Lithic metasandstone, metasiltstone, calcareous metasiltstone, metasandstone, metamudstone, metabasalt, metadolerite and metacarbonate. Low to medium grade.|
30155|Winnama Formation|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Central Zone. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|1845-1840 Ma (Inferred)||||Lithic metasandstone, metasiltstone and calcareous metasiltstone, metamudstone, metabasalt, metadolerite and metacarbonate; low to medium grade, minor amphibolite|
30155|Winnama Formation|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv.|1840-1845 Ma||||Lithic metasandstone, metasiltstone, metamudstone, metabasalt, metadolerite and metacarbonate.|
30155|Winnama Formation|70812|6|Mentioned|p30|||||||||
30155|Winnama Formation|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|1845-1840 Ma (inferred)||||Lithic metasandstone, metasiltstone, metamudstone, metabasalt, metadolerite, and metacarbonate; low to medium grade, calcareous metasiltstone and metasandstone|
30155|Winnama Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Halls Creek Orogen.|||||Lithic metasandstone, metasiltstone, metamudstone, metabasalt, metadolerite, and metacarbonate; low to medium grade.|
30155|Winnama Formation|73089|6|Mentioned|p33|Orosirian|Orosirian|Lamboo Province, Central Zone. Dominantly Paleoproterozoic detritus.|c. 1875-1855 Ma||||Includes metasedimentary units.|
30357|Winnemia Sandstone Member|14228|5|Briefly described|p8|Permian|Permian|Mory and Backhouse (1997).||Callytharra Formation||||06-OCT-16
30357|Winnemia Sandstone Member|67977|5|Briefly described|p480, p481 Fig. 2, p482, p485-7, p489|Sakmarian|Sakmarian|Sand prone facies. Fossils rare in this interval of Callytharra Formation. Geol. Prov: Byro Sub-basin, Southern Carnarvon Basin||Callytharra Formation|||Sandstone.|18-SEP-14
30357|Winnemia Sandstone Member|72910|3|Fully described|p1, p8,p14,p15,21,  p40-42.|Sakmarian|Sakmarian|Only recognised in Jimba Jimba Syncline area.  Thickness approx 100m. Type section runs across the northeast end of the syncline where the only complete, non-faulted section of the unit is present at 25deg02'10""S, 114deg59'30""E. Restricted to exposures  previously assigned to Moogooloo Sandstone. Marine shelf environment envisaged.||Callytharra Formation|||Massive fine to medium-grained sandstone with rare bioturbation.|18-FEB-21
30357|Winnemia Sandstone Member|73623|6|Mentioned|p16|||"Merlinleigh Basin. The rank (Member) is not stated; the unit is ""designated within the formation"". Represents a progradational phase with the influx of quartz sand."||Callytharra Formation||||
74660|Wirku Metamorphics|64722|6|Mentioned|Fig. 2 p3-6, p17|||Informal unit? Oldest exposed unit in the western Musgrave Orogen.||||||
74660|Wirku Metamorphics|65135|5|Briefly described|p1, p5, p6 Fig.4, p7 Fig.5, p10-11, p13|Ectasian|Ectasian|Oldest exposed rocks in the Musgrave Complex. Gneisses of sedimentary and lesser volcaniclastic and volcanic origin. Maximum deposition ages between ~1360 and 1307 Ma. Shows evidence of extensive recrystallisation during the Musgravian Orogeny.||||||
74660|Wirku Metamorphics|65693|6|Mentioned|p3 Fig.1.|||||||||
74660|Wirku Metamorphics|65833|4|Described|p1, p5, p6-7 Figs.4-5, p10-11, p13|Ectasian|Ectasian|In Musgrave Complex. Includes rocks formerly grouped as Birksgate, Wirku or Pity Palya Metamorphics. Sedimentary and lesser volcaniclastic and volcanic gneisses with pelitic, arkosic and quartzitic interlayers. Depositional age ~1360 to c.1307 Ma, coeval with Wankanki Supersuite granites (1336-1293 Ma). Extensively recrystallised during Musgravian Orogeny, destroying fabrics developed during Mount West Orogeny.||||||
74660|Wirku Metamorphics|65898|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province. 1360-1293 Ma. Medium- to coarse-grained garnet-sillimanite pelitic gneiss; medium-grained orthopyroxene-plagioclase(-quartz) acid to intermediate granulite gneiss.||||||
74660|Wirku Metamorphics|65906|6|Mentioned|p3|Ectasian|Ectasian|Formed during the 1336-1293 Ma Mount West Orogeny.||||||
74660|Wirku Metamorphics|65907|5|Briefly described|pp3-5, p8, p11.|||West Musgrave Complex. Comprises much of the basement. Granulite facies metapelites with migmatitic layering from Mount West Orogeny c.1336 Ma - c.1293 Ma.|Deposition between c.1360 and 1307 Ma.||||Felsic gneisses; metapelites. Feldspar porphyroblasts form minor but important component.|
74660|Wirku Metamorphics|66241|5|Briefly described|p28.|||West Musgrave Province. Sediments were deposited over a wide region between 1360 and 1307 Ma, prior to intrusion by granites of the 1336 - 1293 Ma Wankanki Supersuite.||||Intruded by Wankanki Supersuite, in part.||02-DEC-13
74660|Wirku Metamorphics|66256|5|Briefly described|p4 Fig.3, p5 Fig.4, p6, p8, see comments|Stenian|Ectasian|In west Musgrave Province. Interpreted to have protoliths of sedimentary and lesser volcaniclastic and volcanic origin. Detrital zircon ages discussed in some detail. SHRIMP metamorphic age (source GSWA): Mamutjarra Zone 1119+/-7 to 1184+/-5 Ma; Tjuni Purlka Tectonic Zone 1028+/-23 to 1298+/-26 Ma; Walpa Pulka Zone 1170+/-8 to 1214+/-7 Ma. See also p11 Fig.8, p13, p29 Fig.26, p53-54 App.1.||||Veins and sheets of Tjuni Purlka suite cut and engulf rocks of Wirku Metamorphics.|Thinly interbedded or laminated arkosic metasandstone, pelitic (garnet-sillimanite-hercynite-cordierite) gneiss.|11-JAN-17
74660|Wirku Metamorphics|66280|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Map shows six unnamed units, aged 1360-1293 Ma. Various gneisses: metatexitic, diatexitic, granulite, composite; some interlayered with psammitic, pelitic, quartzitic or volcaniclastic layers. ||||||
74660|Wirku Metamorphics|66281|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province.|||||Weakly to strongly banded gneiss.|
74660|Wirku Metamorphics|66282|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Is mapped as nine separate but un-named units of differing lithologies.|1360 - 1293 Ma.||||A variety of gneisses, granulites, migmatites; pelitic, psammitic and calc-silicate rocks.|
74660|Wirku Metamorphics|66284|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Mapped as 15 separate, un-named units.|1360 - 1293 Ma.||||Includes banded gneiss, metatexitic gneiss, strongly migmatitic quartzofeldspathic granulitic paragneiss, acid to intermediate granulite; mostly of sedimentary or volcanosedimentary protolith but includes felsic to mafic intrusive protolith.|
74660|Wirku Metamorphics|67128|5|Briefly described|p6-8, p15, p17-18, p31|||Western Musgrave Province. Variations in ages of detrital zircons, relative to Musgrave Province Zones, are detailed. Dominant detrital sediment source produced 1600-1500 Ma; deposited during the c.1345-1293 Ma Mount West Orogeny. Zircon rim growth records metamorphism at 1127 +/- 9 Ma and 1119 +/- 7 Ma (Kirkland et al., 2010).||||Is overlain unconformably by MacDougall Formation.|Metamorphosed arkosic and psammitic paragneisses; mylonitic, granulite facies.|
74660|Wirku Metamorphics|67244|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Mapped as six separate but un-named sub-units.|1340 - 1270 Ma.||||Metatexitic, psammitic, pelitic gneisses; diatexitic coarse-grained pelite; strongly migmatitic quartzo-feldspathic granulitic paragneiss; acid to intermediate granulite gneiss; metagranodiorite and metamonzogranite.|
74660|Wirku Metamorphics|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave province. Mapped as 21 separate but un-named units.|1340 - 1270 Ma.||||Undivided: weakly to strongly banded gneiss; typically quartzofeldspathic but includes amphibolitic rocks; mostly of sedimentary or volcanosedimentary protolith.|
74660|Wirku Metamorphics|67375|3|Fully described|p6, pp8-9 Fig.5, p13, pp22-23, pp76-123|Mesoproterozoic|Mesoproterozoic|Named after local name for a series of small hills (Wirku Wirku) 5 km northeast of Mount Fanny. Protoliths were deposited in the Ramarama Basin, West Musgrave Province. Supracrustal packages (now mainly paragneiss) previously thought to be exposed basement. Now includes rocks previously grouped as the Piti Palya Metamorphics. Includes interlayers of, and detritus from, volcanic units of the Wankanki Supersuite. Underwent ultra-high temperature metamorphism during the Musgrave Orogeny. Lithology is described in detail.|1340-1270 Ma (Evins et al. 2011).|||Forms inclusions in Pitjantjatjara and Wankanki Supersuite granites. Includes Wankanki Supersuite rocks.|Psammites, migmatitic arkosic metasandstones, pelites, lesser metavolcaniclasatic and metavolcanic rocks; rare calc-silicate layers; strongly deformed into composite gneisses with granoblastic textures|
74660|Wirku Metamorphics|67553|4|Described|p8-9,11-12,15-17,19,22-26,28,31,43|Ectasian|Ectasian|Geological province: Musgrave Province, North Australian Craton. Of Ramarama Basin. Supracrustal packages (now paragneiss) exposed in SA previously thought to be part of the Birksgate Complex. Protoliths are likely sedimentary and lesser volcaniclastic and volcanic origin and deposited in Walpa Pulka, Tjuni Purlka and Mamutjara zones. Intruded by Wankanki Supersuite, thereby constraining depositional age of the protoliths to between 1340 and 1293 Ma (Smithies et al., 2009; Evins et al., in prep.). Large-scale folding related to SE-NW compression at ?1293-M1220 Ma (post tectonic intrusion of Pitjantjatjara intrusions across NE trending folds; GSWA 184146 and 185610)). Contains distinct detrital zircon component age trends: mainly 1650-1530 Ma, dominant 1750 ma in Walpa Pulka; 1580-1450 Ma, dominant c. 1520 Ma and significant c. 1370 and 1320 Ma zircons from the Wankanki Supersuite in Tjuni Purlka; c. 1345-1293 Wankanki Supersuite zircons and older than c. 1410 Ma zircons in Mamutjarra. Dominance of medium-grained and quartz-rich lithologies and absence of pelitic units would suggest that protoliths were deposited in proximal regions of submarine fans. See also p59,70,73,75,91,95.|1340-1270 Ma||||Dominantly banded pelites, psammites, and migmatitic paragneisses, with local continuous layering and containing pelitic, arkosic, and near-orthoquartzitic interlayers.|
74660|Wirku Metamorphics|67888|6|Mentioned|p61||||||||Paragneiss.|
74660|Wirku Metamorphics|68077|5|Briefly described|p1, p3-4, p23-24, p30, p32-33, p35-36|Mesoproterozoic|Mesoproterozoic|See also p38, p42. Howard et al. (2011). Age is minimum age of deposition. Isotopic composition (Lu-Hf and Sm-Nd) and evolution tabulated and discussed in detail.|c. 1300 Ma|||Interleaved with Wankanki Supersuite.|Paragneiss, leucogranite, pelitic gneiss, felsic gneiss, mafic granulite, migmatite.|07-SEP-17
74660|Wirku Metamorphics|68100|4|Described|p1, 2, 3, 4 7-16, 22, 24-27,29,31,32-36|Mesoproterozoic|Mesoproterozoic|Called Wirku Metamorphics in west Musgrave Province, but grouped into Birksgate Complex elsewhere. Together with the Wankanki Supersuite forms the Ramarama Basin.Aeromagnetic and gravimetric lows in comparison with Pitjantjatjara and Warakurna Supersuites. Numerous SHRIMP dates have been derived from samples of this unit, the age given here is the maximum range for most of the ages given for sedimentary protoliths deposition. Metamorphic event ages also discussed.|1340-1214 Ma (SHRIMP)|||Intruded by Wankanki Supersuite ~1345-1293 Ma. Disconformably overlain by MacDougall Formation at Mt Blythe.|Pelitic gneisses. Pelitic rocks.  Gneissic rocks, granulite facies metamorphics with granoblastic textures. Arkosic metasandstones, psammitic rock with pelitic layers, composite gneisses, granitic gneiss, paragneiss and garnet leucogranites.|
74660|Wirku Metamorphics|68995|6|Mentioned|p3 Fig.1, p4 Fig.2, p6||||c. 1340-1270 Ma|||Unconformably overlain by the Kunmarnara Group.||
74660|Wirku Metamorphics|68996|5|Briefly described|p2, 3, 4, 24, 27-29, 35-46, 48-49, 59||||||||Granulite facies paragneiss and metasedimentary rocks.|
74660|Wirku Metamorphics|69003|5|Briefly described|p4, p37-38|Mesoproterozoic|Mesoproterozoic|Ramarama Basin, W Musgrave Province, Paterson Orogen. Sediments sourced from the Gawler and South Australian Cratons.|1340-1270 Ma.||||Psammitic and minor pelitic metasedimentary rocks; locally interlayered with volcanic rocks.|
74660|Wirku Metamorphics|69091|5|Briefly described|p52 Fig.4.1, p54 Fig.4.2, see comments|||Musgrave Province. Sedimentary protolith deposited in Ramarama Basin. Oldest outcropping supracrustal gneissic rocks are assigned to the Wirku Metamorphics and are found in the Walpa Pulka, Tjuni Purlka and Mamutjarra Zones of the west Musgrave Province. Recent work has shown that much of what was previously regarded as exposed basement in the west Musgrave Province (see Birksgate Complex) actually comprises supracrustal packages (now mainly paragneiss) deposited between c. 1340 Ma and 1270 Ma (Evins et al., 2012) - referred to as Wirku Metamorphics (Howard et al., 2007; Evins et al., 2009; Smithies et al., 2009). Shown as Wirku metamorphics in Fig.6.4 and Fig.6.5 legends. See also p55 Fig.4.3, p56, p59 Fig.4.6, p60-63, p65-66, p72, p86, p131 incl. Fig.6.1, p137-139 Figs.6.4-6.6, p141 Fig.6.8, p142, p183.|1340-1270 Ma|||Sedimentary protoliths were intruded by Wankanki Supersuite granites; is unconformably overlain by Kunmarnara Group|Banded gneiss, mainly preserved as rafts in granite; gneiss interpreted to have protoliths of sedimentary and lesser volcaniclastic and volcanic origin.|
74660|Wirku Metamorphics|69153|5|Briefly described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Paterson Orogen, Musgrave Province. Several Geochron samples of unnamed parts of Wirku Metamorphics have been anaylsed and these records are found in GEOCHRON section of reference.|||||Weakly to strongly banded gneiss; typically quartzofeldspathic, includes amphibolitic rocks; mostly derived from sedimentary or volcanosedimentary protoliths; locally intruded by granite; interlayered with felsic volcanic and volcaniclastic units|02-SEP-14
74660|Wirku Metamorphics|69436|6|Mentioned|p21:2, 5|Mesoproterozoic|Mesoproterozoic||1340-1270 Ma.|||||12-JUL-16
74660|Wirku Metamorphics|69655|5|Briefly described|p3, p6, p9, p37, p66, p77-p78|Ectasian|Ectasian|Musgrave Province.|c. 1340-1270 Ma||||Paragneisses.|
74660|Wirku Metamorphics|69729|5|Briefly described|p66 Fig.1, p68-72, p74-76, p84, p88-89|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Protoliths (arkosic sandstones, mudstone, quartz-rich sandstone, felsic volcanics) were deposited after c.1340 Ma (Evins et al., 2012). Occurs as rafts in granites, including the Wankanki Supersuite. The granofelses are chemically similar to the Wankanki Supersuite granites. Regional geochronological variations detailed.|1340-1270 Ma.||||Banded paragneisses, metapelitic schist, orthoquartzite; local fine-grained granofelsic units (felsic volcanics).|
74660|Wirku Metamorphics|70083|6|Mentioned|p206|||||||||
74660|Wirku Metamorphics|70084|4|Described|p219-221,223-226|Ectasian|Ectasian|Geological province: Musgrave Province, Paterson Orogen. Associated with Mount West Orogeny and coeval with Wankanki Supersuite, and Recherche Supersuite and Fraser Range Metamorphics in the Albany-Fraser Orogen. Clastic protoliths were deposited into Ramarama Basin, accompanied by minor volcanic additions from contemporaneous Wankanki magmatism (Evins et al., 2012). Samples from the Latitude Hills area indicate considerably evolved isotopic signatures with TDM2 ages greater than 2.6 Ga, and zircons detrital populations with peaks at 2622, 2713, and 2838 Ma, and several minor components between 3096 and 1524 Ma. Wirku Metamorphics EHfi values: WMa: EHfi= 0 to +10; 1.3-1.6 Ga (falls along an evolution line from 1.9 Ga and 1.6 Ga mantle extraction events, and overlaps the fields for Papulankutja,Wankanki and Pitjantjatjara Supersuites (Kirkland et al., 2013a); WMb: EHfi= -10 to -30; 2.0-1.6 Ga indicating reworking of WMc component); WMc: EHfi= +7 to -10, (3.3 Ga; reflecting Archean detritus from Latitude Hills region and U-Pb 3.0-2.2 crystallisation age).|||||Banded paragneisses.|09-JUN-20
74660|Wirku Metamorphics|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|Musgrave Province/(complex?) SHRIMP dates from migmatitic metasandstone (174748.1.pdf) and garnet paragneiss (183596.1.pdf). Incorporates all units that were once grouped into the Birksgate Metamorphics (or Birksgate Complex), Piti Palya and Wirku Metamorphics groups (184149.1.pdf).|1083 Ma +/- 63 Ma,  1667 Ma (SHRIMP) |Musgrave Complex|||Granofels, Banded gneiss, amphibolitic rocks, metatexitic gneiss, pelitic and psammitic gneiss, psammite, quartzite, pelite, migmatite, paragneiss, leucogranite, quartzofeldspathic gneiss, granulite,  felsic volcaniciclastic rocks, granulite gneiss.|
74660|Wirku Metamorphics|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Metamorphosed to granulite facies during late stages (1190-1165 Ma) of the Musgrave Orogeny. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma); Musgrave Orogeny (1220-1150 Ma); Mount West Orogeny (1345-1293 Ma). Sample GSWA 174588 (migmatitic metasandstone) yielded an interpreted (regression intersecting concordia curve) maximum depositional age of 1394+\-26 Ma, and metamorphic zircon rim growth at 1193+\-10 Ma. Sample GSWA 174748 (migmatitic metasandstone) yielded an interpreted (weighted mean 207Pb*/206Pb*) maximum depositional age of 1377+\-33 Ma for the sandstone, and zircon rim growth at 1214+\-7 Ma (contact metamorphism with the intrusive Pitjantjatjara Supersuite) and 1170+\-8 Ma (2nd metamorphic event). Sample GSWA 183466 (banded gneiss) yielded an (207Pb*/206Pb*) interpreted maximum depositional age of 1385+\-23 Ma for the sedimentary protolith, metamorphic zircon rim growth (weighted mean 207Pb*/206Pb*) at 1221+\-7 Ma and migmatisation (207Pb*/206Pb*) at 1083+\-64 Ma. Sample GSWA 183596 (laminated paragneiss) yielded an interpreted (weighted mean 207Pb*/206Pb*) maximum depositional age of 1272+\-15 Ma for the sedimentary protolith, and a high-grade metamorphic event dated (weighted mean 207Pb*/206Pb*) at 1161+\-7 Ma. Sample GSWA 184590 (metasandstone) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) maximum depositional age of 1310+\-7 Ma for the sandstone, or if the protolith is a mylonitised granite, then that date would represent igneous crystallisation age; and a high-grade metamorphic (concordia) date of 1172+\-14 Ma. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv + other geochron files for additional geochronological sample analyses.|1340-1270 Ma (inferred); 1336+\-11 Ma; 1317+\-9 Ma|||Intruded by Pitjantjatjara Supersuite and Wankanki Supersuite.|Composite gneiss of pelite, psammite,feldic volcanics and felsic to intermediate granulite gniess, migmatite, quartzofeldspathic gneiss and paragneiss, granofels.|
74660|Wirku Metamorphics|70826|6|Mentioned|p10|Mesoproterozoic|Mesoproterozoic|||||||
74660|Wirku Metamorphics|70831|5|Briefly described|p2-p3, p5, p20|||Ramarama Basin.|c. 1340-1270 Ma||||Metasedimentary and metavolcanic rocks.|
74660|Wirku Metamorphics|70839|6|Mentioned|p326|||Geological province: Musgrave Province.||||||
74660|Wirku Metamorphics|71088|6|Mentioned|p5|||Musgrave Province.|c. 1340-1270 Ma|||||
74660|Wirku Metamorphics|71169|5|Briefly described|p80|Ectasian|Ectasian|Western Musgrave Province. Deposited during the Mount West Orogeny. May have been deposited in a continental arc or contains an inherited arc signature.|1340-1270 Ma||||Arc-like felsic extrusive rocks.|
74660|Wirku Metamorphics|71170|5|Briefly described|p5-p6, p9, p23, p41|Mesoproterozoic|Mesoproterozoic|West Musgrave Province. Protoliths were interpreted to be sedimentary with a lesser volcaniclastic to volcanic component.|1340-1270 Ma||||Gneissic metasedimentary rocks.|
74660|Wirku Metamorphics|71210|5|Briefly described|p4-p5, p7, p21, p23|||Musgrave Province. Protoliths of this unit are interpreted to be pelitic to psammitic sedimentary rocks with depositional ages of c.1340-1300 Ma. See also p51, p53, p67, p80-p81, p113.|||||Quartzofeldspathic, peraluminous paragneisses.|
74660|Wirku Metamorphics|71211|5|Briefly described|p6, p7 fig 1.4, p24 fig 2.1, p84 fig 3.1|||Musgrave Province. Age is of protolith deposition. See also p136 fig 4.1, p228. |1340-1270 Ma||||Banded gneiss, preserved as rafts within granites.|
74660|Wirku Metamorphics|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma); Musgrave Orogeny (1220-1150 Ma); Mount West Orogeny (1345-1293 Ma). Commonly metamorphosed to granulite facies. Sample GSWA 174588 (opx-bearing quartzofeldspathic gneiss) yielded a concordia curve age of 1193+\-10 Ma, interpreted as the age of zircon rim growth during peak metamorphism; and a 207Pb/206Pb date of 1394+\-26 Ma, interpreted as maximum depositional age of sedimentary protolith. Sample GSWA 174748 (migmatitic metasandstone) yielded a weighted mean 207Pb/206Pb date of 1377+\-33 Ma, interpreted as the maximum depositional age of sedimetary protolith; and weighted mean 207Pb/206Pb ages of 1214+\-7 Ma and 1170+\-8 Ma, indicating episodes of metamorphic zircon rim growth. Sample GSWA 174797 (foliated paragneiss) yielded a weighted mean 207Pb/206Pb date of 1173+\-8 Ma, interpreted as the crystallization age for the anatexic component of the gneiss. Sample GSWA 183466 (banded gneiss) yielded a weighted mean 207Pb/206Pb interpreted maximum depositional age of sedimentary protolith of 1385+\-24 Ma, and metamorphism at 1221+\-7 Ma and migmatisation at 1083+\-24 Ma. Sample GSWA 183596 (laminated paragneiss) yielded a weighted mean 207Pb/206Pb age of 1272+\-15 and 1161+\-7 Ma, interpreted as maximum depositional age of sedimentary protolith and a high-grade metamorphic event respectively. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv.|1340-1270 Ma (inferred)||||Composite gneiss; pelite and psammite with intermediate granulite; pelite, quartzofeldpsathic gneiss, granofels,metasiliciclastics and metafelsic volcaniclastics, granultie gneiss.|
74660|Wirku Metamorphics|71321|4|Described|p5,10|Ectasian|Ectasian|Geological province: Musgrave Province. Defined on the western Musgrave Province as a younger (than Birksgate Complex) supracrustal package of mostly paragneisses. Deformed and metamorphosed at amphibolite to granulite facies during the province-wide c. 1220-1120 Ma Musgravian Orogeny (Edgoose, et al., 2004; Major and Conor, 1993; Smithies, et al., 2010).|c. 1340-1270 Ma|||Near synchronous with Wankanki Supersuite.|Paragneisses.|
74660|Wirku Metamorphics|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1193+/-10 Ma (metamorphism: U-Pb zircon SHRIMP)||||Migmatitic metasandstone, stromatic migmatite, laminated paragneiss, psammite, banded and laminated quartzofeldspathic paragneiss, felsic paragneiss, quartzite, granitic/pelitic gneisses.|
74660|Wirku Metamorphics|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Musgrave Province, Paterson Orogen.|||||Undivided weakly to strongly banded gneiss; typically quartzofeldspathic but includes amphibolitic rocks; mostly derived from sedimentary or volcano-sedimentary protoliths.|
74660|Wirku Metamorphics|72094|5|Briefly described|p2, p3 Fig 2|Ectasian|Ectasian|Musgrave Province. Volcano-sedimentary rocks interpreted as syn- or post-orogenic sequence within the Ramarama Basin. Underwent UHT metamorphism during Musgrave Orogeny.|1340-1270 Ma||||Paragneiss|
74660|Wirku Metamorphics|72443|6|Mentioned|p737|Mesoproterozoic|Mesoproterozoic|Musgrave Province.|1340-1270 Ma|||||
74660|Wirku Metamorphics|73058|5|Briefly described|p760, p761 Fig.1, p770-771, p776, p778|Ectasian|Ectasian|Musgrave Province. Protolith included detrital zircon age ranges of c. 3200-2630 Ma, 1790-1590 Ma, 1570-1470 Ma. Hf and Nd model ages suggest crust formation and juvenile additions at c. 1900 Ma, 1650-1550 Ma. Detrital zircon Hf isotopic values occur in several distinct radiogenic and non-radiogenic groups. Protolith formed from Musgrave Province basement including an Archean component being uplifted, eroded and redeposited, same age as Wankanki Supersuite. Location in text includes p772 Fig.8-9, p773-774.|c. 1345-1293 Ma, 1340-1270 Ma||||Paragneisses.|
74660|Wirku Metamorphics|73346|6|Mentioned|p5|||Musgrave Province. Mount West Orogeny.||||||
74660|Wirku Metamorphics|73437|5|Briefly described|p151, p153|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Deposited as volcano-sedimentary rocks during Mount West Orogeny.|1340-1270 Ma||||Paragneiss.|
24115|Withnell Formation|12491|6|Mentioned|p454 Fig.7.|Late Cretaceous|Late Cretaceous|Presented in figure as Korojon, Withnell, Toolonga Formations. Carbonates.||||||06-NOV-14
24115|Withnell Formation|40617|5|Briefly described|p15|||||||||
24115|Withnell Formation|40800|2|Defined|p10|early Maastrichtian|early Campanian|Early Campanian to Early Maastrichtian.||||||30-JUN-14
24115|Withnell Formation|41271|3|Fully described|p158|||||||||
24115|Withnell Formation|41438|6|Mentioned|p109|||||||||
24115|Withnell Formation|41439|5|Briefly described|p123|||||||||
24115|Withnell Formation|41732|6|Mentioned|Fig.3|||||||||
24115|Withnell Formation|42116|5|Briefly described|Fig.1 P6|||||||||
24115|Withnell Formation|43712|5|Briefly described|p12||Cretaceous|||||||
24115|Withnell Formation|43722|6|Mentioned|p11||Cretaceous|||||||
24115|Withnell Formation|43724|5|Briefly described|p30||Cretaceous|||||||
24115|Withnell Formation|43826|6|Mentioned|Fig.2,p163||Late Cretaceous|||||||01-MAR-10
24115|Withnell Formation|44938|4|Described|p151, Fig.3||Late Cretaceous|Campanian age.||||||01-SEP-08
24115|Withnell Formation|62734|5|Briefly described|p1362 Fig. 2|Late Cretaceous|Late Cretaceous|Geological Province: Barrow Sub-basin.||||||01-SEP-08
24115|Withnell Formation|62837|5|Briefly described|Stratigraphic columns|Late Cretaceous|Late Cretaceous|Age: >75->65Ma. Geological Province: Dampier Sub-basin, Rankin Platform, Beagle Sub-basin and Roebuck Basin.||||||01-MAR-10
24115|Withnell Formation|63950|5|Briefly described|p336 Fig. 4|Maastrichtian|Campanian|Geological Province: northern Carnarvon Basin.||||||27-MAY-08
24115|Withnell Formation|67368|6|Mentioned|p209 Fig.4.|Maastrichtian|Campanian|||||Overlies Toolonga Calcilutite.||
24115|Withnell Formation|69692|6|Mentioned|p4|Late Cretaceous|Late Cretaceous|Northern Carnarvon Basin.||||Overlies Toolonga Calcilutite. Is overlain by Miria Marl.||
24115|Withnell Formation|70066|5|Briefly described|Dampier: Fig.2. Exmouth: Fig.2|Maastrichtian|Campanian|See also Regional: Fig.6. Northern Carnarvon Basin.||||Overlies Toolonga Calcilutite. Is overlain by Miria Formation.||
24115|Withnell Formation|70906|5|Briefly described|p757-758|Late Cretaceous|Late Cretaceous|Gorgon Platform.||||Overlies Toolonga Calcilutite. Is overlain by Dockrell Formation.||
24115|Withnell Formation|73564|6|Mentioned|p1225|Cretaceous|Cretaceous|Exmouth Sub-basin.||||Overlies Toolonga Calcilutite. Correlated with Korojon Calcilutite.||
24116|Woblegun Formation|23594|4|Described|p20|Mesoproterozoic|Mesoproterozoic|Of Manganese Subgroup. Underlain by Pinjian Chert Breccia. Geological Province: Bangemall Basin.||||||24-JUL-07
24116|Woblegun Formation|24025|4|Described|p15|Mesoproterozoic|Mesoproterozoic|Of  Manganese Group.  Geological Province: Collier Basin.||||||
24116|Woblegun Formation|24110|5|Briefly described|Plate 1|Proterozoic|Proterozoic|Parent: Manganese Group.  Geological Province: Collier Basin||||||
24116|Woblegun Formation|41669|2|Defined|Table 5|Proterozoic?||Fully described p37.||||||24-JUL-07
24116|Woblegun Formation|42352|6|Mentioned|p31|||||||||
24116|Woblegun Formation|43055|3|Fully described|Table 4, Table 5|||Of the Manganese Group.||||||24-JUL-07
24116|Woblegun Formation|43056|5|Briefly described|Map Legend|||of Manganese Group||||||
24116|Woblegun Formation|44142|5|Briefly described|p315, 316 Tb.4-4, p322-323|||Up to 280m thick marine shelf deposits. Probably a marine equivalent of coeval Coondoon Formation. Base of Manganese Subgroup; restricted to E of Oakover River.||Manganese Subgroup||Overlain conformably by Stag Arrow Formation.|Shale, micaceous siltstone; minor sandstone, glauconitic sandstone, conglomerate, chert.|
24116|Woblegun Formation|44831|5|Briefly described|Map Legend||Proterozoic|||||||
24116|Woblegun Formation|60535|5|Briefly described|p556 Fig.1|Mesoproterozoic|Mesoproterozoic|Of the Manganese Group (Bangemall Formation).||||||
24116|Woblegun Formation|63417|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Manganese Group (Bangemall Supergroup).  Geological Province: Collier Basin. Interbedded shale, siltstone, sandstone and conglomerate; local dolostone and stromatolitic dolostone.||||||
24116|Woblegun Formation|65829|5|Briefly described|p27.|Mesoproterozoic|Mesoproterozoic|A siliciclastic and carbonate succession about 95 km southeast of the Ripon Hills. Originally part of the superseded Bangemall Group. Contains glauconitic sandstone towards the top of its succession.||Stated to be a unit in Manganese Group and also of the Collier Group.||||
24116|Woblegun Formation|66107|5|Briefly described|p4 Fig.1|Mesoproterozoic|Mesoproterozoic|||Of the Manganese Group||Is overlain by Whitewood Formation.||
24116|Woblegun Formation|67183|5|Briefly described|p645, p649 Fig.8|Mesoproterozoic|Mesoproterozoic|See also Williams (1989) and Williams (1990).||Manganese Subgroup||Unconformably overlies the Mount Bruce Supergroup and granite-greenstones of the Pilbara Craton, lateral equivalent to the Coondoon Formation.|<280 m thick (eastern Oakover Basin), shales, siltstone and poorly sorted fine-grained sandstone units.|
24116|Woblegun Formation|67202|4|Described|p52, p54, p64, p258|Mesoproterozoic|Mesoproterozoic|Collier Basin. c.300m thick. Shallow near-shore marine, or lagoonal, deposits. Deformed into broad open folds disrupted by NNW-trending faults by the Miles or Paterson Orogenies. Poorly magnetised: not discriminated in aeromagnetic data.||Manganese Group.||Unconformably overlies Pinjian Chert Breccia and Fortescue Group. Is intruded by Davis Dolerite. Is overlain unconformably by Googhenama Formation (Tarcunyah Group).|Interbedded shale, siltstone, sandstone and conglomerate; local dolostone and stromatolitic dolostone.|15-FEB-18
24116|Woblegun Formation|69167|4|Described|geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|||Manganese Group|||Dolostone; partly stromatolitic; sandstone, pebbly sandstone, conglomerate and siltstone; medium to coarse grained;|13-AUG-18
24116|Woblegun Formation|69590|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Events: Western Australian events. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|1465-1070 Ma (inferred)|Unit of Manganese Group.|||Dolostone; partly stromatolitic; sandstone, siltstone, conglomerate.|
24116|Woblegun Formation|71042|5|Briefly described|p67|Mesoproterozoic|Mesoproterozoic|Oakover Basin. < 280 m thick. Interpreted as a marine-shelf deposit.||Manganese Group||Equivalent to the Coondoon Formation. Overlies the Mount Bruce Supergroup.|Shales, siltstone and poorly sorted fine-grained sandstone.|24-MAY-19
24116|Woblegun Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||sandstone, conglomerate, chert, shale|
24116|Woblegun Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Collier Basin. ||Manganese Group|||Sandstone and siltstone; medium to coarse grained; thin beds of conglomerate.|
74839|Wogala Suite|64891|5|Briefly described|p37 Fig. 2, p42, p52-53 Tb. 1|Archean|Archean|Of Bald Rock Supersuite. Includes Marlomumbah Granite. Age: c.2625Ma. Geological province: Murchison Domain. Fluorite-bearing alkali granites; post-tectonic. Referred to as a Granite Suite in Fig. 2.||||||07-FEB-11
74839|Wogala Suite|65548|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Bald Rock Supersuite, Yilgarn Craton. Includes Marlomumbah Granite.||||||
74839|Wogala Suite|66195|5|Briefly described|p599 Fig.2|Neoarchean||In the Bald Rock Supersuite. Granitic.||||||13-MAR-12
74839|Wogala Suite|67129|6|Mentioned|p18 fig 19|Archean|Archean|Murchison Domain, Youanmi Terrane.||Bald Rock Supersuite|||Granites.|07-SEP-17
74839|Wogala Suite|68519|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c. 2610 Ma|Of the Bald Rock Supersuite.|||Monzogranite, muscovite-rich granite and muscovite-bearing pegmatite; all metamorphosed.|
74839|Wogala Suite|68561|5|Briefly described|GEOL_LUT_CSV folder + GEOCHRON files|||Murchison Domain, Youanmi Terrane. ||Bald Rock Supersuite|Includes Marlomumbah Granite||Includes muscovite-bearing pegmatite, locally fluorite and lepidolite bearing; metamorphosed|
74839|Wogala Suite|68698|5|Briefly described|p4-5, p6 Tb.1, p8, p10, p14-17, p27-28|Neoarchean|Neoarchean|Post-tectonic, undeformed granites. Magmatic crystallisation age of a biotite-muscovite-fluorite granite. Geochemistry is discussed. REE plots.|2606 +/- 5 Ma (Wingate et al., 2011).|Bald Rock Supersuite.|||Fluorite-bearing alkali granite.|
74839|Wogala Suite|69583|4|Described|p49, p51, p99; Plate 2|Neoarchean|Neoarchean|Murchison Domain.|2610-2600 Ma.|Bald Rock Supersuite.|Marlomumbah Granite.|Intrudes Windimurra Igneous Complex.|Fluorite-bearing alkali granite; lithium-rich pegmatites.|
74839|Wogala Suite|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean|||Bald Rock Supersuite|Marlomumbah Granite|||
74839|Wogala Suite|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Bald Rock Supersuite.|Marlomumbah Granite.|||
74839|Wogala Suite|70020|5|Briefly described|p118|Neoarchean|Neoarchean|Geological province: Yilgarn Craton.||Unit of Bald Rock Supersuite.||Underlain by Walganna Suite.||
74839|Wogala Suite|70030|5|Briefly described|p192|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton.||Unit of Bald Rock Supersuite.||||
74839|Wogala Suite|70419|5|Briefly described|p10|||||Bald Rock Supersuite.||Crosscuts lower Windimurra Igneous Complex.|Includes Li-rich pegmatites.|
74839|Wogala Suite|70796|4|Described|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton granite. See also 100k_geologyp_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 185928.1.pdf, 207630.1.pdf, Madoonga100_2444_stratig.pdf, Windimurra100_2641_stratig.pdf.|2625 to 2600 Ma (inferred)|Bald Rock Supersuite|||Muscovitebearing alkali granite; equigranular; common accessory fluorite; posttectonic|
74839|Wogala Suite|70830|5|Briefly described|p9|||Murchison Domain.||Bald Rock Supersuite||||
74839|Wogala Suite|71168|5|Briefly described|p7|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c. 2610-2600 Ma|Bald Rock Supersuite|||Granitic rocks.|
74839|Wogala Suite|71269|5|Briefly described|GEOL_LUT_CSV files|||Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.||Unit of Bald Rock Supersuite.|Includes Marlomumbah Granite.|||
74839|Wogala Suite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|||Bald Rock Supersuite|Includes Marlomumbah Granite.||Muscovite-bearing alkali granite; equigranular; common accessory fluorite; post-tectonic.|
38599|Wolline Monzogranite|23783|5|Briefly described|p88|Archean|Archean|Of the Muccan Granitoid Complex.  Age: 3244+/-3Ma.||||||07-NOV-08
38599|Wolline Monzogranite|44229|5|Briefly described|Map legend|Archean|Archean|Of the Muccan Granitoid Complex.  Porphyritic and seriate monzogranite and syenogranite; pink-grey, medium- to coarse-grained.  Age: c.3244-3252Ma.||||||07-NOV-08
38599|Wolline Monzogranite|50383|5|Briefly described|Map Legend|Archean|Archean|Of Muccan Granitoid Complex. Age: c. 3252-3244 Ma. Geological Province: Pilbara Craton||||||07-NOV-08
38599|Wolline Monzogranite|50544|5|Briefly described|p29, p19 Tb. 2 (amended)|Archean|Archean|Of the Muccan Granitoid Complex.  Age: 3244+/-3Ma.||||||07-NOV-08
38599|Wolline Monzogranite|50555|5|Briefly described|Map legend|Archean|Archean|Of the Muccan Granitoid Complex.  Porphyritic and seriate monzogranite and syenogranite; pink-grey, medium to coarse-grained.  Age: 3252-3244Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
38599|Wolline Monzogranite|60429|2|Defined|p6 Fig. 3, p16,  p36 Appdx. 1|Archean|Archean|Youngest plutons in the Muccan Granitoid Complex. Age: c.3252-3244Ma (Nelson 1998). Geological Province: Pilbara Craton. Pink-grey, porphyritic to seriate, medium- to coarse-grained monzogranite and syenogranite.||||||07-FEB-11
38599|Wolline Monzogranite|63420|5|Briefly described|Map legend|Archean|Archean|Of the Cleland Supersuite.  Age: 3250Ma. Geological Province: Pilbara Craton. Porphyritic to seriate monzogranite; grades to syenogranite; pink-grey, medium- to coarse-grained; local flow-banding and igneous mineral alignment, pegmatite banding...........||||||07-NOV-08
38599|Wolline Monzogranite|63441|5|Briefly described|p9 Tb. 2|Archean|Archean|Of the Cleland Supersuite. Ages: 3252+/-3Ma and 3244+/-3Ma. Geological province: Pilbara Craton.||||||07-FEB-11
38599|Wolline Monzogranite|64936|5|Briefly described|map legend|Archean|Archean|Of Muccan Granitoid Complex. Monzogranite and syenogranite; metamorphosed. Age: c. 3250 Ma (geochronology: Nelson DR in prep). Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
38599|Wolline Monzogranite|66217|4|Described|p5, pp34-35.|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Ages from Nelson (1998d) and Williams (1999) respectively; other samples returned ages of 3251 +/- 2 Ma and 3250 +/- 2 Ma (Nelson, 2005c,d).|3252 +/- 3 Ma and 3244 +/- 3 Ma.|Unit in Cleland Supersuite.||Intrudes Pilbara Supergroup.|Weakly-deformed, porphyritic and seriate monzogranite and syenogranite; medium- to coarse-grained, leucocratic.|
38599|Wolline Monzogranite|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c.3250 Ma|Of the Cleland Supersuite.|||Porphyritic to seriate monzogranite; grades to syenogranite; pink-grey, medium to coarse grained; local flow banding and igneous mineral alignment, pegmatite banding, or other foliation locally with inclusions of schlieric metatonalite.|
38599|Wolline Monzogranite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Age derived from samples of porphyritic biotite granite and porphyritic biotite granodiorite (143810.1.pdf, 178022.1.pdf)|3244 Ma +/- 3 Ma - 3315 +/- 3 Ma  (SHRIMP)|Cleland Supersuite|||Monzogranite, leucocratic monzogranite with schlieric tonalite inclusions and syenogranite; porphyritic and seriate; all metamorphosed.|
38599|Wolline Monzogranite|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA 143810 (porphyritic bt monzogranite) yielded an interpreted crystallisation age of  3244+\-3 Ma of the monzogranite (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3251-3244 Ma (isotopic, inferred)|Unit of Cleland Supersuite.|||Monzogranite and syenogranite; leucocratic, porphyritic and seriate; metamorphosed|
38599|Wolline Monzogranite|70022|6|Mentioned|p113, 116-117, 119|||Part of Cleland Supersuite. East Pilbara Terrane. Presented also as Wolline Granodiorite on p116. Archean zircons described; CL image.|3250 +/- 2 Ma.|Muccan Granitic Complex.|||Granodiorite. Includes a banded tonalite gneiss enclave.|
38599|Wolline Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, syenogranite|
38599|Wolline Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||Max age 3252+/-3 Ma, Min 3244+/-3 Ma|Cleland Supersuite|||Monzogranite and syenogranite; porphyritic and seriate; metamorphosed.|
83902|Wombola Dolerite|70087|5|Briefly described|p215, 217-218, 220, 222-223|Archean|Archean|Wombola Domain, the western part of the Daisy Milano mining camp. Gold-mineralised quartz veins cut through the unit. Photograph, photomicrograph.|||||A ~150m thick mineralised sill; made up of amphibole-quartz-plagioclase-biotite. Displays boudinage of mineral grains and clusters.|
80380|Wonangara Member|72712|4|Described|p22, p57, p9 Fig.5, p23, p24, p27, p43.|Rhyacian|Rhyacian|Appearing as four separate outcrops of diamictite within the lower 450 m of the Kazput Formation, along the northern limb of the Hardey Syncline.||Kazput Formation||Unconformably underlies Munder Formation.|Diamictite. Shown as consisting predominantly of fine'grained siliciclastic rocks as well as local thin to very thick carbonate interbeds, but is generally poorly exposed.|
34888|Wongarlong Formation|22907|6|Mentioned|41|||Misspelling of Wongarling?||||||
34888|Wongarlong Formation|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Of Tarcunyah Group, Officer Basin.||||||
34888|Wongarlong Formation|23590|2|Defined|p13, p22 Appendix 2|||Age: <840 Ma (poor age constraints). Of Tarcunyah Group. Overlying unit Tchukardine Formation. Underlying unit Yandanunyah Formation. Officer Basin. Max. thickness: ~1200 m.||||||
34888|Wongarlong Formation|23729|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Tarcunyah Group. Geological Province; Paterson Orogen.||||||
34888|Wongarlong Formation|23730|4|Described|p11|Neoproterozoic|Neoproterozoic|Of Tarcunyah Group. Overlying unit Nooloo Formation. Underlying unit Brownrigg Sandstone. Geological Province: Officer Basin.||||||
34888|Wongarlong Formation|23760|4|Described|p29|Neoproterozoic|Neoproterozoic|Of Tarcunyah Group. Geological Province: Officer Basin.||||||
34888|Wongarlong Formation|50008|5|Briefly described|p46 Fig.3||Neoproterozoic|Of Tarcunyah Group. Geological Province: Officer Basin.||||||
34888|Wongarlong Formation|60470|5|Briefly described|p4 Fig. 2|Neoproterozoic|Neoproterozoic|in Officer Basin, of Tarcunyah Group. Sandstone; minor conglomerate, siltstone, and shale||||||
34888|Wongarlong Formation|62453|4|Described|p5 Fig. 3, 61, 66|Cryogenian|Cryogenian|Geological Province: Paterson Orogen. Underlies: Tchukardine Formation unconformably. Thickness: ~1200m. Sandstone, siltstone, shale. ||||||
34888|Wongarlong Formation|64580|6|Mentioned|map legend|||Of Tarcunyah Group.||||||15-DEC-08
34888|Wongarlong Formation|64777|5|Briefly described|p3 Fig.4 |Neoproterozoic|Neoproterozoic|||Of the Tarcunyah Group|||Sandstone; minor conglomerate, siltstone and shale.|
34888|Wongarlong Formation|65454|4|Described|p7 Fig.3, p10, p30 Fig.A1b|Neoproterozoic|Neoproterozoic|Of Tarcunyah Group. Medium- to fine-grained sandstone interbedded with laminated and micaceous siltstone and shale forming upward-coarsening successions, also associated with restricted basalt or fine grained dolerite. Overlies Yandanunyah Formation.|of Group ~850-830 Ma.|||||30-AUG-18
34888|Wongarlong Formation|65826|6|Mentioned|p7 Fig.4. |Neoproterozoic|Neoproterozoic|Officer Basin.||Unit in Tarcunyah Group.||||
34888|Wongarlong Formation|67202|4|Described|p64-65, p125, p231|Neoproterozoic|Neoproterozoic|NW Officer Basin. Over 1200m thick. Shallow-marine shelf deposits. Appears as the Wangarlong Formation on p64.||Tarcunyah Group.||Conformably overlies Yandanunyah Formation. Is overlain conformably by Nooloo Formation.|Fine- to medium-grained sandstone and orthoquartzite with gypsum casts, interbedded with laminated siltstones and shale.|15-FEB-18
34888|Wongarlong Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|NW Paterson Orogen.||Tarcunyah Group.||||
34888|Wongarlong Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|Neoproterozoic|Neoproterozoic|||Unit of Tarcunyah Group.||||
34888|Wongarlong Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone, basalt|
34888|Wongarlong Formation|72034|5|Briefly described|500k_interpgeop16_lut|Cryogenian|Tonian|Gibson Sub-basin, Officer Basin (Phase 1).||Tarcunyah Group|||Medium-grained sandstone, siltstone, shale; local evaporite pseudomorphs.|
26231|Wongawol Formation|7161|6|Mentioned|p99 Fig.9|||Earaheedy Basin. Approximately 1500m thick (from p99 Fig.9).||||||
26231|Wongawol Formation|22493|5|Briefly described|p99 Fig.9|||||||||
26231|Wongawol Formation|22969|4|Described|Fig 4.1b|Late Permian|Late Permian|Of the Sydney Subgroup.||||||17-JUL-08
26231|Wongawol Formation|23529|4|Described|p21|Paleoproterozoic|Paleoproterozoic|Of the Miningarra Subgroup. Thickness: ~<1500m. Geological Province: Earaheedy Basin.||||||07-NOV-08
26231|Wongawol Formation|23530|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Miningarra Subgroup, Earaheedy Basin||||||07-NOV-08
26231|Wongawol Formation|23589|5|Briefly described|p2 Fig 2|||Of Miningarra Subgroup. Overlain by Kulele Limestone. Underlain by Princess Ranges Member. Geological Province: Earaheedy Basin.||||||17-JUL-08
26231|Wongawol Formation|23611|6|Mentioned|p24|||||||||
26231|Wongawol Formation|23890|5|Briefly described|p21 Fig.11|||Of Miningarra Subgroup. Geological Province: Earaheedy Basin.||||||
26231|Wongawol Formation|24017|5|Briefly described|p3 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Miningarra Subgroup.  Geological Province: Earaheedy Basin.||||||07-NOV-08
26231|Wongawol Formation|24578|4|Described|p776 Fig.1, p781|Paleoproterozoic|Paleoproterozoic|Of the Miningarra Subgroup (Earaheedy Group). Overlain by the Kulele Limestone. Overlies the Chiall Formation. Geological Province: Earaheedy Basin.||||||07-NOV-08
26231|Wongawol Formation|30010|6|Mentioned|p45|||||||||
26231|Wongawol Formation|31217|2|Defined|p42|Paleoproterozoic|Paleoproterozoic|Mention p40.||||||07-NOV-08
26231|Wongawol Formation|36551|6|Mentioned|Table 29|||||||||
26231|Wongawol Formation|37021|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26231|Wongawol Formation|37300|6|Mentioned|p82|||||||||
26231|Wongawol Formation|37460|3|Fully described|p142|||||||||
26231|Wongawol Formation|38515|4|Described|p14|||||||||
26231|Wongawol Formation|38516|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26231|Wongawol Formation|38978|3|Fully described|p167|||||||||
26231|Wongawol Formation|38988|6|Mentioned|Fig.2|||||||||
26231|Wongawol Formation|40354|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26231|Wongawol Formation|40355|5|Briefly described|p7|||||||||
26231|Wongawol Formation|40934|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26231|Wongawol Formation|40938|2|Defined|p55|Paleoproterozoic|Paleoproterozoic|Mention p13.||||||07-NOV-08
26231|Wongawol Formation|40939|5|Briefly described|p108|||||||||
26231|Wongawol Formation|41997|6|Mentioned|Fig.2 P73|||||||||
26231|Wongawol Formation|43595|5|Briefly described|Table 3-9,p346|||||||||
26231|Wongawol Formation|43652|6|Mentioned|Fig.3,p381|||||||||
26231|Wongawol Formation|50188|5|Briefly described|p2 Fig. 1, p3|||Of the Miningarra Subgroup (Earaheedy Group). Conformably overlies Chiall Formation. Maximum Thickness: ~1500m.  Geological Province: Earaheedy Basin.||||||16-JUL-08
26231|Wongawol Formation|50222|4|Described|p320 Fig. 3, p329|Paleoproterozoic|Paleoproterozoic|Of the Miningarra Subgroup (Earaheedy Group).  Iron-rich shale, siltstone to very fine-grained sandstone, intraclastic breccia and carbonate-glauconite breccia.  Max. thickness: <1500m.  Geological Province: Earaheedy Basin.  See also p319 Fig. 2.||||||07-NOV-08
26231|Wongawol Formation|50223|5|Briefly described|p345 Fig. 2, p346|Paleoproterozoic|Paleoproterozoic|Of the Miningarra Subgroup (Earaheedy Group).  Shale, siltstone to very fine-grained sandstone, intraclastic breccia, glauconitic carbonate breccia.  Conformably overlies Princess Ranges Member.  Geological Province: Earaheedy Basin.||||||07-NOV-08
26231|Wongawol Formation|50224|5|Briefly described|p368 Tb.1|Paleoproterozoic|Paleoproterozoic|Of the Minningarra Subgroup (Earaheedy Group).  Arkosic and lithic sandstone; siltstone, minor carbonate in upper part. Max. thickness: ~1000m. Geological Province: Earaheedy Basin.||||||07-FEB-11
26231|Wongawol Formation|50226|5|Briefly described|p423, p424 Fig. 5|||Of the Miningarra Subgroup (Earaheedy Group). Fine clastic and carbonate beds. Geological Province: Earaheedy Basin.  See also p426.||||||26-MAY-09
26231|Wongawol Formation|50378|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Miningarra Subgroup (Earaheedy Group). Geological Province: Earaheedy Basin.  Very fine grained sandstone, siltstone, shale. minor intraclastic sandstone and carbonate rock breccia; locally glauconitic.||||||07-NOV-08
26231|Wongawol Formation|63866|5|Briefly described|p166|||Eraheedy Basin.||Miningarra Subgroup||Overlies the Chiall Formation. Overlain by the Kulele Limestone.||
26231|Wongawol Formation|64284|4|Described|p58 Fig. 1, p60 Fig. 2, p61|Paleoproterozoic|Paleoproterozoic|Of the Minningarra Subgroup (Earaheedy Group). Geological Province: Earaheedy Basin. Shale, siltstone to very fine-grained sandstone, intraclastic breccia, and carbonate-glauconite breccia. Thickness: <1500m.||||||07-FEB-11
26231|Wongawol Formation|64285|5|Briefly described|p65, p66-67 Figs.1,2|Paleoproterozoic|Paleoproterozoic|Of Minningarra Subgroup (Earaheedy Group). Geological Province: Earaheedy Basin. Shale, siltstone and fine-grained sandstone.||||||07-FEB-11
26231|Wongawol Formation|64580|4|Described|map legend||Paleoproterozoic|Of Miningarra Subgroup. Sandstone, shale, dolomite, dolomitic siltstone, and conglomerate.||||||09-DEC-08
26231|Wongawol Formation|64725|6|Mentioned|p59.|||||Unit in Miningarra Subgroup.||Overlies Chiall Formation. Is overlain by Kulele Limestone.||
26231|Wongawol Formation|64772|4|Described|p12, Plate 1, p10 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of Miningarra Subgroup (Earaheedy Gp). Max. thickness: 1500m (may be exaggerated by faulting, folding?). Prospective for manganese mineralization. Earaheedy Basin. On Plate 1,  unit is of Earaheedy Group (as Miningarra Subgroup not shown).. See also p19 Fig.9, p20-21 Fig.10, p26 Fig.13, p43, p44, p51, p69 App.4, p75 App.4 Tb.4.3, p76-77 Fig.4.2, p78 App.4 Tb.4.4, p79-81 App.4 Fig.4.3.||||overlies Chiall Formation (contact is highest medium-grained sandstone); is overlain gradationally by Kulele Limestone|Arkosic and lithic sandstone, thin-bedded siltstone, shale, mudstone, intraclastic breccia, and carbonate-glauconite breccia; carbonate bands increase in abundance higher in the sequence; volcaniclastics towards top interpreted as distal ashfall.|25-NOV-13
26231|Wongawol Formation|65264|6|Mentioned|p32|||Contains stratiform iron- and manganese-oxide bands.||||||07-FEB-11
26231|Wongawol Formation|65472|5|Briefly described|p1, p3 Fig.2|||Thickness: ~1500 m. Earaheedy Basin.||Miningarra Subgroup|||fine-grained clastic and carbonate rocks; minor ash-tuff beds|
26231|Wongawol Formation|65692|5|Briefly described|p9-11, p55|||Low energy shallow-marine environment with far-field ashfall deposits. c.1500m thick. Unusual thickness possibly related to deformation during formation of the Stanley Fold Belt. ||Miningarra Subgroup.||Overlies Chiall Formation. Is overlain by Kulele Limestone.|Includes siltstone, sandstone, carbonate, iron-rich shale, some breccia and a thin volcaniclastic layer. Contains mudcracks and ripple marks.|
26231|Wongawol Formation|66427|5|Briefly described|p43 Fig.2, p45-48, p51, p63, p68-75|||c.1500 m thick. Hosts local stratiform Fe-Mn oxides with anomalous abundances of Cu, Ba and Pb in clastic beds.||Unit in Miningarra Subgroup.||Overlies Chiall Formation; is overlain transitionally by Kulele Limestone.|Monotonous succession of shale, mudstone, siltstone, very fine-grained feldspathic sandstone, and minor intraclast conglomerate.|
26231|Wongawol Formation|67855|6|Mentioned|p208 fig 3-8|Paleoproterozoic|Paleoproterozoic|||Minningarra Subgroup||||
26231|Wongawol Formation|68055|6|Mentioned|p77|Proterozoic|Proterozoic|Earaheedy Basin.||Miningarra Subgroup.||||
26231|Wongawol Formation|69003|5|Briefly described|p13 Fig.17, p14-15|||Earaheedy Basin. c.1500m thick.||Miningarra Group.||Conformably? Overlies Chiall Formation. Is overlain conformably? by Kulele Limestone.|Cleaved and folded, shallow-marine siltstone.|
26231|Wongawol Formation|69152|4|Described|500k_geologyp08_lut||Paleoproterozoic|||Miningarra Subgroup|||Undivided; sandstone, shale, dolomite, dolomitic siltstone, and conglomerate.|07-AUG-15
26231|Wongawol Formation|69313|6|Mentioned|p22 Fig.4.2, p25|Paleoproterozoic|Paleoproterozoic|||Minningarra Subgroup||Overlies the Chiall Formation. Overlain by the Kulele Limestone.||08-SEP-17
26231|Wongawol Formation|69596|6|Mentioned|p10-11|||Earaheedy Basin.||Miningarra Group.||||
26231|Wongawol Formation|70153|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic||1876 +/- 19 Ma (isotopic) - 1600 Ma (inferred).|Miningarra Group|||Sandstone, shale, dolomite, dolomitic siltstone, stromatolitic limestone; minor conglomerate.|
26231|Wongawol Formation|71042|6|Mentioned|p97|||Earaheedy Basin. Hosts high-grade supergene manganese oxide zones with low-grade stratiform iron and manganese oxide bands interbedded with sandstone and siltstone.|||||Interbedded sandstone and siltstone.|
26231|Wongawol Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, shale, mudstone, claystone|
26231|Wongawol Formation|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen, West Australian Craton. of Earaheedy Basin. Events: Edmundian Orogeny (1026 - 954 Ma); Mangaroon Orogeny (1682 - 1619 Ma); Stanley Fold Belt deformation (2005 - 1620 Ma); Mangaroon Orogeny D2m/M2m (1677 - 1659 Ma); Mangaroon Orogeny D1m/M1m (1682 - 1677 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv.|1876+\-19 Ma; 1650 Ma (inferred)||||Sandstone, shale, dolomite, dolomitic siltstone, stromatolitic limestone; minor conglomerate|
26231|Wongawol Formation|71484|4|Described|p124-125,131-132|Orosirian|Orosirian|Geological province: Of Earaheedy Basin. Thickness: c. 1500m. Generally deepens in depositional facies across central part of the basin. Likely depositd in a shallow water setting. Volcaniclastic clasts within a poorly sorted conglomerate show vitriclastic textures andmay represent reworking of nearby volcaniclastic units or contemporaneous volcanism.||Unit of Miningarra Group.||Overlain by Kulele Limestone. Underlain by Chiall Formation.|Siltstone, fine-grained feldspathic sandstone, mudstone and minor conglomerate and stromatolitic limestone.|30-AUG-19
26231|Wongawol Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin.|Max age 1876+/-19 Ma, Min ~1650 Ma.|Miningarra Group|||Sandstone, shale, dolomite, dolomitic siltstone, stromatolitic limestone; minor conglomerate.|
24120|Wongi Basalt|22534|6|Mentioned|p4, Fig.4 p7|||of Pole Group, See also Table 2. p8||||||
24120|Wongi Basalt|22596|6|Mentioned|Fig.9 p419|||||||||
24120|Wongi Basalt|22640|5|Briefly described|p298|||||||||
24120|Wongi Basalt|42221|6|Mentioned|Table 1 P6|||||||||
24120|Wongi Basalt|42382|5|Briefly described|Fig.4 P11|||||||||
24120|Wongi Basalt|42696|6|Mentioned|Plate 1B|Archean||||||||07-NOV-08
24120|Wongi Basalt|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
24120|Wongi Basalt|42870|5|Briefly described|Table 1, P67|||||||||
24120|Wongi Basalt|42989|5|Briefly described|Fig.3|||||||||
24120|Wongi Basalt|43074|6|Mentioned|Fig.4,p16|||||||||
24120|Wongi Basalt|43101|5|Briefly described|p7|||0f Pole Group||||||
24120|Wongi Basalt|43162|6|Mentioned|5|||||||||
24120|Wongi Basalt|43496|6|Mentioned|6|||||||||
24120|Wongi Basalt|43574|6|Mentioned|Fig.1,p298|||||||||
24120|Wongi Basalt|60076|5|Briefly described|p12 Tb. 2|||Variolitic high-Mg basalt.  Max. thickness: >2000m.  Geological Province: Ora Banda domain.||||||
24120|Wongi Basalt|60514|6|Mentioned|p65 Table 1.|Archean|Archean|Of the Pole Group. Overlain by Missouri Basalt. Geological Province: Ora Banda Domain.||||||07-FEB-11
24120|Wongi Basalt|60627|5|Briefly described|p65 Tb.1|||Of Pole Group.||||||
24120|Wongi Basalt|63981|6|Mentioned|p93 Fig.3, |Archean|Archean|Ora Banda Domain. Kambalda Sequence. |||||Tholeiitic and high MgO basalt.|
24120|Wongi Basalt|65204|6|Mentioned|pg6 Tbl.1, p11|Archean|Archean|Unit in Pole Group. Ora Banda Domain. Komatiitic basalt.||||||
24120|Wongi Basalt|65834|6|Mentioned|p7|||Ora Banda Domain, Kalgoorlie Terrane.||Pole Group.||||
24120|Wongi Basalt|70326|5|Briefly described|p360-362|Neoarchean|Neoarchean|Geological province: Ora Banda region, Ora Banda Domain, Kalgoorlie Terrane, Yilgarn Craton. Mg-rich basalt.||||Overlain by Missouri Basalt. Correlable to Hickies Bore Basalt.||
24120|Wongi Basalt|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).  See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2726-2680 Ma (inferred)|Unit of Vetters Subgroup.|||Komatiitic basalt; variolitic to pyroxene spinifex-textured; locally pillowed; metamorphosed; Komatiite; locally preserved olivine-spinifex texture; commonly serpentinized or silicified; schist; talc-chlorite(-carbonate) and tremolite-chlorite.|
24120|Wongi Basalt|73391|5|Briefly described|p53, 279, Appendices.|||Ora Banda Domain, Kalgoorlie Terrane. Shown as having a combined thickness over 3000m with Missouri Basalt.||Pole Group; Lower Basalt.||Overlies Siberia/Owen monzogranites. Is overlain by Walter Williams dunite.|Poorly exposed basalt and amphibolite.|
40569|Wonnerup Member|12758|5|Briefly described|p3 Fig. 3|Late Triassic|Early Triassic|Of the Lesueur Sandstone.  Homogeneous sandstone, feldspathic, poorly sorted, coarse to very coarse-grained, unconsolidated and light grey to colourless. Overlain by the Myalup Member.  Geological Province: Southern Perth Basin.  see also p8 Fig. 9.||||||
40569|Wonnerup Member|14227|5|Briefly described|Enclos. 2|Triassic|Triassic|Of Lesueur Sandstone.||||||07-FEB-11
40569|Wonnerup Member|24443|5|Briefly described|Fig.31|Middle Triassic|Early Triassic|Of Lesueur Sandstone. Conformably overlies Sabina Sandstone. Conformably overlain by Myalup Member. Geological Province: Perth Basin.||||||
40569|Wonnerup Member|50107|5|Briefly described|Map legend|Triassic|Triassic|Of the Lesueur Sandstone.  Geological Province: Southern Perth Basin.||||||
40569|Wonnerup Member|67925|5|Briefly described|Ch2 p10 fig 4, Ch3 p8|Carnian|Scythian|||Lesueur Sandstone||Overlies the Sabina Sandstone. Overlain by the Myalup Member.||
40569|Wonnerup Member|69029|5|Briefly described|p332|Carnian|Anisian|Of Perth Basin.||Unit of Lesueur Sandstone.||||
40569|Wonnerup Member|69081|5|Briefly described|p737 Fig.1|Middle Triassic|Middle Triassic|Geol. Prov: Perth Basin.||Lesueur Sandstone.||Is overlain by Yalgorup Member (Lesueur Sandstone); overlies Sabina Sandstone.||23-JUL-15
40569|Wonnerup Member|69182|6|Mentioned|Ch2 p9, Ch2 p45, Ch2 p51|Late Triassic|Middle Triassic|Perth Basin. ||Lesueur Sandstone||Overlies the Myalup Member.|Clean massive sandstones.|
40569|Wonnerup Member|70097|5|Briefly described|p19 Fig.3|Carnian|Anisian|Southern Perth Basin. Bunbury Trough.||Lesueur Sandstone||Overlies Sabina Sandstone. Is overlain by Myalup Member.|Sandstone.|12-SEP-17
40569|Wonnerup Member|71377|5|Briefly described|p3, p7, p41, p67-p71|Middle Triassic|Middle Triassic|Perth Basin. Intersected in GSWA Harvey 1 (1378-2895m). Interpretedas stacked high energy fluvial deposits with lesser moderate- to low-energy floodplain deposits. See also p77, p85, p87, p90, p102-p103.||Lesueur Sandstone||Conformably overlies the Sabina Sandstone. Overlain by the Yalgorup Member.|Poorly sorted, relatively homogeneous, feldspathic, coarse to very coarse-grained, light grey coloured sandstone.|
40569|Wonnerup Member|71958|5|Briefly described|p34|Ladinian|Olenekian|Vlaming Sub-basin.||Lesueur Sandstone||Overlies the Sabina Sandstone. Overlain by the Myalup Member.||
27257|Wonyulgunna Sandstone|22478|6|Mentioned|p23||Mesoproterozoic|Bangemall Group, Bangemall Basin||||||
27257|Wonyulgunna Sandstone|22694|6|Mentioned|p8|||Collier Subgroup, Bangemall Basin||||||
27257|Wonyulgunna Sandstone|22940|4|Described|p21|Mesoproterozoic|Mesoproterozoic|Edmund Subgroup, Bangemall Basin. Overlying unit: Backdoor Formation (U)||||||
27257|Wonyulgunna Sandstone|23156|5|Briefly described|p8|Mesoproterozoic|Mesoproterozoic|Overlying unit on BULLEN - Backdoor Formation (conformity)||||||
27257|Wonyulgunna Sandstone|23597|5|Briefly described|p11|||Of Bangemall Group.||||||
27257|Wonyulgunna Sandstone|23723|6|Mentioned|p8 Fig 4|||Geological Province: Bangemall Basin.||||||
27257|Wonyulgunna Sandstone|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Bangemall Group. Geological Province: Bangemall Basin.||||||
27257|Wonyulgunna Sandstone|24017|4|Described|p23|||Parent: Collier Group.||||||
27257|Wonyulgunna Sandstone|24018|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Collier Subgroup. Geological Province: Bangemall Basin.||||||
27257|Wonyulgunna Sandstone|24183|6|Mentioned|p20|||Overlain by the Backdoor Formation.||||||
27257|Wonyulgunna Sandstone|24535|5|Briefly described|p4 Fig.2|Mesoproterozoic|Mesoproterozoic|Of Collier Group.||||||
27257|Wonyulgunna Sandstone|33849|4|Described|p126|||||||||
27257|Wonyulgunna Sandstone|37018|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27257|Wonyulgunna Sandstone|37026|4|Described|p4|||||||||
27257|Wonyulgunna Sandstone|37460|6|Mentioned|p172|||||||||
27257|Wonyulgunna Sandstone|37707|6|Mentioned|Table I|||||||||
27257|Wonyulgunna Sandstone|38298|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27257|Wonyulgunna Sandstone|38299|4|Described|p12|||||||||
27257|Wonyulgunna Sandstone|38515|4|Described|p15|||||||||
27257|Wonyulgunna Sandstone|38516|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27257|Wonyulgunna Sandstone|40089|2|Defined|p44|Mesoproterozoic|Mesoproterozoic|||||||
27257|Wonyulgunna Sandstone|40989|4|Described|p33|||||||||
27257|Wonyulgunna Sandstone|43209|5|Briefly described|map legend||Mesoproterozoic|Of Collier Subgroup.||||||
27257|Wonyulgunna Sandstone|43238|5|Briefly described|p7|||||||||
27257|Wonyulgunna Sandstone|43830|5|Briefly described|Map Legend||Mesoproterozoic|||||||
27257|Wonyulgunna Sandstone|44142|5|Briefly described|p315 Tb.4-4, p321-322|||~800m thick lenticular beach or fluvial deposits.||Collier Subgroup||Overlies unconformably the Earaheedy Group. Overlain by Backdoor Formation conformably.|Quartz arenite; minor cobble conglomerate, siltstone, shale, chert.|
27257|Wonyulgunna Sandstone|50195|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Scorpion Group. Quartz sandstone and subordinate siltstone.  Geological Province: Scorpion Basin.||||||23-JUN-04
27257|Wonyulgunna Sandstone|50334|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Collier Group (Bangemall Supergroup). Geological Province: Bangemall Superbasin.||||||
27257|Wonyulgunna Sandstone|50626|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Collier Subgroup (Bangemall Group).  Quartz sandstone.  Geological Province: Bangemall Basin.||||||
27257|Wonyulgunna Sandstone|60535|5|Briefly described|p556 Fig.1|Mesoproterozoic|Mesoproterozoic|Of the Collier Group (Bangemall Supergroup).||||||21-MAR-11
27257|Wonyulgunna Sandstone|63869|6|Mentioned|p40|Mesoproterozoic|Mesoproterozoic|Not present in western Bangemall Supergroup.||Basal unit in Collier Group.||||
27257|Wonyulgunna Sandstone|64580|4|Described|map legend||Mesoproterozoic|Of Scorpion Group. quartz sandstone;  minor cobble conglomerate, siltstone, and mudstone.||||||09-DEC-08
27257|Wonyulgunna Sandstone|64772|5|Briefly described|p13, Plate 1, p25 Fig.12, p33 Fig.21|Mesoproterozoic|Mesoproterozoic|Of the Scorpion Group; previously of Collier Group. Quartz sandstone; minor cobble conglomerate, siltstone and mudstone.||||||25-NOV-13
27257|Wonyulgunna Sandstone|65896|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Lower Collier Group, Bangemall Supergroup. Quartz sandstone and feldspathic quartz sandstone; locally includes minor shale.||||||
27257|Wonyulgunna Sandstone|69003|5|Briefly described|p36|Mesoproterozoic|Mesoproterozoic|Crops out at Ingebong Hills, Capricorn Orogen. Exhibits dramatic giant cross-beds.||Scorpion Group.||||
27257|Wonyulgunna Sandstone|70795|4|Described|500k_interpgeop14_lut.csv|Mesoproterozoic|Paleoproterozoic||1620-1080 Ma||||Quartz sandstone, minor cobble conglomerate, siltstone and mudstone.|
27257|Wonyulgunna Sandstone|71158|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Scorpion Basin.|1653-1455 Ma.|Scorpion Group.|||Quartz sandstone; minor cobble conglomerate, siltstone and mudstone.|
27257|Wonyulgunna Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone, conglomerate, evaporite|
27257|Wonyulgunna Sandstone|71269|4|Described|1m_geologyp12_lut.csv|||Geological province: Capricorn Orogen; West Australian Craton. ||Unit of Scorpion Group.|||Coarse to medium grained white quartz sandstone, siltstone with numerous pyrite pseudomorphs, shale and minor conglomerate; rippled and cross bedded. Minor evaporite.|
27257|Wonyulgunna Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Paleoproterozoic|Scorpion Basin.||Scorpion Group|||Quartz sandstone; minor cobble conglomerate, siltstone, and mudstone.|
26232|Woodada Formation|12758|5|Briefly described|p8 Fig. 9|Late Triassic|Middle Triassic|Transitional between Lesueur Sandstone above and Kockatea Sandstone below.  Not recognised in the Southern Perth Basin. Geological Province: Northern Perth Basin.||||||11-APR-08
26232|Woodada Formation|14227|5|Briefly described|p7-8, p10|Early Triassic|Early Triassic|Fluvial deposits. Underlies Lesueur Sandstone. See also Enclosure 2.||||||07-FEB-11
26232|Woodada Formation|14228|5|Briefly described|p5 fig 2, p8, p16, p17|Triassic|Triassic|Possible oil source rock.||||Overlies Kockatea Shale. Overlain by Lesueur Sandstone.||06-OCT-16
26232|Woodada Formation|23172|4|Described|Map Legend|Triassic|Triassic|||||||
26232|Woodada Formation|23279|4|Described|p20,23|Anisian|Scythian|||||||
26232|Woodada Formation|23520|5|Briefly described|p6 Fig. 4|Middle Triassic|Early Triassic|Marine claystone, siltstone.  Max. thickness: 715m.Geological Province: Abrolhos Sub-basin.  See also p9 and 12.||||||
26232|Woodada Formation|23816|4|Described|p238|Middle Triassic|Scythian|Geological Province: Perth Basin. Underlying unit: Kockatea Shale (conformable). Overliyng unit: Lesueur Sandstone (disconformable). Max. thickness: 276 m.||||||27-APR-05
26232|Woodada Formation|24058|5|Briefly described|p115|||Geological Basin: Perth Basin.||||||
26232|Woodada Formation|24160|6|Mentioned|p94|Triassic|Triassic|||||||
26232|Woodada Formation|24351|5|Briefly described|Plate 3, Plate 4 (in pockets)|Middle Triassic|Middle Triassic|Geological Province: Gascoyne Platform/Sub-basin. Log Wittecarra-1.||||||13-DEC-07
26232|Woodada Formation|24390|5|Briefly described|p15 Fig. 8|Triassic|Triassic|Geological Province: Perth Basin.||||||
26232|Woodada Formation|24443|5|Briefly described|p22, Fig.30|Middle Triassic|Early Triassic|Conformably overlies Kockatea Shale. Overlain by Lesueur Sandstone.  Geological Province: Perth Basin.||||||03-FEB-05
26232|Woodada Formation|29633|6|Mentioned|p435|||Permian/Triassic boundary||||||
26232|Woodada Formation|29693|6|Mentioned|Fig.7|||||||||
26232|Woodada Formation|29721|6|Mentioned|Table 226|||||||||
26232|Woodada Formation|29790|6|Mentioned|p92|||||||||
26232|Woodada Formation|30565|6|Mentioned|Fig.4|||||||||
26232|Woodada Formation|31238|5|Briefly described|p28|||See also Fig. 12A||||||
26232|Woodada Formation|31562|6|Mentioned|p10|||Stratigraphic table||||||
26232|Woodada Formation|31568|5|Briefly described|p19|||M. Triassic||||||
26232|Woodada Formation|31910|3|Fully described|Table 1|||See Table 1||||||
26232|Woodada Formation|32165|6|Mentioned|p196|||Sections correlated BMR10 & 10A||||||
26232|Woodada Formation|32376|6|Mentioned|p1542|||||||||
26232|Woodada Formation|32648|6|Mentioned|p32|||L.-M. Triassic||||||
26232|Woodada Formation|32714|6|Mentioned|Fig.2|||||||||
26232|Woodada Formation|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
26232|Woodada Formation|33386|6|Mentioned|Fig.7|||||||||
26232|Woodada Formation|34008|4|Described|p76|||Triassic. See also PP69,73,75||||||
26232|Woodada Formation|34009|6|Mentioned|Table III|||||||||
26232|Woodada Formation|34841|6|Mentioned|Fig.2|||||||||
26232|Woodada Formation|35282|6|Mentioned|Fig.2|||||||||
26232|Woodada Formation|35573|6|Mentioned|Fig.13|||Generalised stratigraphy - Perth Basin||||||
26232|Woodada Formation|35653|6|Mentioned|p1093|||Discussion of stratigraphy and basin development. See also Fig.3.||||||
26232|Woodada Formation|35901|6|Mentioned|Table 1|||||||||
26232|Woodada Formation|35968|6|Mentioned|Table 4|||||||||
26232|Woodada Formation|36257|6|Mentioned|Table 2.1|||||||||
26232|Woodada Formation|36265|5|Briefly described|Fig.3.26|Middle Triassic|Early Triassic|Geological Province: Perth Basin.||||||11-APR-08
26232|Woodada Formation|36293|2|Defined|p128|Middle Triassic|Early Triassic|Late Early Triassic to Middle Triassic.E - M||||||
26232|Woodada Formation|36890|3|Fully described|p238|||||||||
26232|Woodada Formation|36911|6|Mentioned|p58|||||||||
26232|Woodada Formation|37104|6|Mentioned|Fig.3|||||||||
26232|Woodada Formation|39155|6|Mentioned|p18|||See also Table 2||||||
26232|Woodada Formation|40992|6|Mentioned|Fig.5|||||||||
26232|Woodada Formation|41172|4|Described|p124|||||||||
26232|Woodada Formation|41192|6|Mentioned|Fig.5|||||||||
26232|Woodada Formation|41195|6|Mentioned|p327|||||||||
26232|Woodada Formation|41284|5|Briefly described|p89|||||||||
26232|Woodada Formation|41728|6|Mentioned|p441|||||||||
26232|Woodada Formation|41729|6|Mentioned|p454|||||||||
26232|Woodada Formation|42075|5|Briefly described|Fig.7 P247|||||||||
26232|Woodada Formation|43031|4|Described|p15,Fig.2|||||||||
26232|Woodada Formation|43062|5|Briefly described|Table 2,p18|||||||||
26232|Woodada Formation|43096|5|Briefly described|p7|||||||||
26232|Woodada Formation|43197|5|Briefly described|Map Legend||Triassic|||||||
26232|Woodada Formation|43216|5|Briefly described|Map Legend||Triassic|Perth Basin||||||
26232|Woodada Formation|43217|5|Briefly described|Map Legend||Triassic|Perth Basin||||||
26232|Woodada Formation|43296|5|Briefly described|Map Legend||Triassic|||||||
26232|Woodada Formation|43297|4|Described|p9,Fig5 p9.|Middle Triassic|Early Triassic|see also Table1 p6.Type section location given.||||||
26232|Woodada Formation|43323|14|Not recorded|p71|||Aratrisporites||||||
26232|Woodada Formation|43347|4|Described|4|Middle Triassic|Early Triassic|||||||
26232|Woodada Formation|43495|4|Described|2-26||Scythian|||||||
26232|Woodada Formation|43504|4|Described|4-10|Anisian|Scythian|||||||
26232|Woodada Formation|44144|4|Described|p507 Tb.4-21, p509 Fig.4-145, p513|Middle Triassic|Early Triassic|Type Section: BMR 10 (Beagle Ridge) 334-610m. 276m thick fluvial deposits.||||Conformably overlies Kockatea Shale. Overlain conformably by Lesueur Sandstone.|Grey, fine- to medium-grained sandstone interbedded with dark-grey laminated siltstone.|
26232|Woodada Formation|44307|2|Defined|p11,15-17||Triassic|U/lies Lesueur Sandstone; O/lies Kockatea Shale. Lower-Middle Triassic.||||||
26232|Woodada Formation|48614|14|Not recorded|p5,31,46, Pl.1,8,9|||(New name). (H50-5,9).||||||
26232|Woodada Formation|48857|2|Defined|p.12||Triassic|O/lain by Cockleshell Gully Sandstone. See p.13.||||||
26232|Woodada Formation|49942|5|Briefly described|p4 Fig.3|Middle Triassic|Middle Triassic|Conformably overlies Kockatea Shale. Conformably overlain by Lesueur Sandstone. Geological Province: Gascoyne Platform.||||||
26232|Woodada Formation|50085|5|Briefly described|p15 Fig. 8|Triassic|Triassic|Age: <250Ma.  Geological Province: Northern Perth Basin.||||||11-MAY-04
26232|Woodada Formation|50107|5|Briefly described|Map legend|Triassic|Triassic|Geological Province: Northern Perth Basin.||||||
26232|Woodada Formation|60376|6|Mentioned|p38, p43-46.|Triassic|Triassic|Geological Province: Perth Basin.  Overlain by Lesueur Sandstone.||||||07-FEB-11
26232|Woodada Formation|60377|5|Briefly described|p61 Fig. 3, p62|Anisian|Scythian|Overlain by Lesueur Sandstone. Underlain by Kockatea Shale. Geological Province: Perth Basin. Deltaic depositional environment.Consists of sandstone with interbedded carbonaceous shales and siltstones.||||||30-APR-13
26232|Woodada Formation|60384|5|Briefly described|p244, p243 Fig 2a, p254, p260 table2|Middle Triassic|Middle Triassic|Perth Basin. Minor fluorescence in one well.|||||Sands and silts|
26232|Woodada Formation|60386|6|Mentioned|p299|Late Triassic|Early Triassic|Perth Basin. Non-marine. Includes volcanics dated 246 +/-7 Ma.||||||
26232|Woodada Formation|61023|5|Briefly described|p20 Fig 10|Triassic|Triassic|Geological Province: Perth Basin.||||||11-APR-08
26232|Woodada Formation|61546|6|Mentioned|p383, p385 Fig.5, p386, p388.|||Marine deposits. Has small reverse faults and folds.||||Overlies Kockatea Shale. Is overlain by Lesueur Sandstone.||
26232|Woodada Formation|61811|5|Briefly described|p3 Fig.2, p66.|Anisian|Olenekian|Northern Perth Basin. Type section details in Appendix 1.||||Overlies Kockatea Shale. Is overlain by Lesueur Sandstone.||
26232|Woodada Formation|63929|6|Mentioned|p131 Fig.2.|Early Triassic|Early Triassic|Perth Basin.||||Overlies Kockatea Shale. Is overlain by Lesueur Sandstone.||
26232|Woodada Formation|64580|4|Described|map legend|Middle Triassic|Early Triassic|Fine- to medium-grained sandstone, interbedded with laminated siltstone.||||||09-DEC-08
26232|Woodada Formation|64635|5|Briefly described|p4 Fig.3 |Anisian|Olenekian|||||Overlies Kockatea Shale. Is overlain by Lesueur Sandstone.||
26232|Woodada Formation|66124|4|Described|p169, p170 Fig.2|Olenekian|Olenekian|Perth Basin. Overlies Kockatea Shale, underlies Lesueur Sandstone. Deltaic sedimentation: fine-grained sandstone and siltstone, up to 230m thick.||||||
26232|Woodada Formation|67135|5|Briefly described|p5 Fig.7.|Triassic|Triassic|Perth Basin.||||Overlies Kockatea Shale. Is overlain by Lesueur Sandstone.||
26232|Woodada Formation|67340|6|Mentioned|p6-8, 25, 50, 52-63|Early Triassic|Early Triassic|Northern Perth Basin. Thermal rock properties. Wells in this unit used for this Report are listed.||||||
26232|Woodada Formation|67370|5|Briefly described|p316, p318. |Early Triassic|Early Triassic|A regressive unit.||||Overlies the Arranoo Member of the Kockatea Shale. Is overlain by Lesueur Formation.||
26232|Woodada Formation|67925|5|Briefly described|Ch4 p8 fig 2|Middle Triassic|Middle Triassic|Northern and central Perth Basin. ||||Overlies the Kockatea Shale. Overlain by the Lesueur Sandstone.||
26232|Woodada Formation|69029|6|Mentioned|p332|Anisian|Anisian|Of Perth Basin.||||Overlain by Lesueur Sandstone. Underlain by Kockatea Shale.||
26232|Woodada Formation|69182|6|Mentioned|Ch2 p3, Ch2 p9, Ch2 p34-p41|Early Triassic|Early Triassic|Perth Basin. Deposited in a shallow marine to coastal environment. Good reservoir qualities, but ultimately lacks a proper sealing unit. See also Ch2 p44-p46, Ch2 p50, Ch2 p51, Ch2 p54-p55, Ch2 p57, Ch2 p60-p67, Ch2 p69, Ch2 p73-p74, Ch2 p83, Ch2 p85-p88, Ch2 p92, Ch2 p94-p96, Ch2 p98-p100, Ch2 p102, Ch2 p104, Ch2 p106, Ch2 p108-p110, Ch3 p12. ||||Overlies the Kockatea Shale. Overlain by the Lesueur Sandstone.||
26232|Woodada Formation|69297|6|Mentioned|p202, p234|||Perth Basin. Deposited in a fluvial-deltaic environment.  ||||||
26232|Woodada Formation|70097|5|Briefly described|p2, p20-22 Figs.4-6|Anisian||Regression; deltaic and fluvial facies of Woodada Formation and Lesueur Sandstone. Northern Perth Basin. Greenough/Bookara Shelf, Dongara Saddle and Dandaragan Trough.||||Overlies Kockatea Shale. Is overlain by Lesueur Sandstone.|Includes shale.|13-SEP-17
26232|Woodada Formation|70128|5|Briefly described|p449, p457, p459, p461-462|Middle Triassic|Middle Triassic|Northern Perth Basin. Modelled thickness distribution histogram.||||Conformably overlies Kockatea Shale. Is overlain conformably by Lesueur Sandstone.||
26232|Woodada Formation|70826|6|Mentioned|p7 tbl 4|Triassic|Triassic|Perth Basin.||||||
26232|Woodada Formation|71146|5|Briefly described|p6|Middle Triassic|Early Triassic|Perth Basin.||||Overlies the Kockatea Shale. Overlain by the Lesueur Sandstone.|Sandstone.|
26232|Woodada Formation|72034|5|Briefly described|500k_interpgeop16_lut|Middle Triassic|Early Triassic|Perth Basin.  Age from biostratigraphy.|||||Fine- to medium-grained sandstone, interbedded with laminated siltstone.|
26232|Woodada Formation|72258|5|Briefly described|p129|Middle Triassic|Middle Triassic|Of Perth Basin.||||Overlain by, and laterally grades southward into Lesueur Sandstone. Underlain by Sabina Sandstone or Kockatea Shale.||
26232|Woodada Formation|73513|5|Briefly described|p30 Fig.2|Anisian|Scythian|Perth Basin.||||Overlies Kockatea Shale, underlies Lesueur Formation|Sandstone.|
79249|Woodada Sequence|69297|6|Mentioned|p204, p206, p209|Middle Triassic|Lower Triassic|Perth Basin. Several units within this sequence have good source richness and potential for both oil and gas. See also p223, p225, p236, p237, p238. ||||Overlies the Kockatea Sequence. Overlain by the Lesueur Sequence.||
79249|Woodada Sequence|70097|5|Briefly described|p3, p4|Late Triassic|Early Triassic|Subsidence, offshore northern Perth Basin. Fluvio-deltaic systems.||||||20-OCT-15
36851|Woodbrook Formation|23484|4|Described|p10 table 3|Archean|Archean|Of Whundo Group.  Maximum thickness: ~1000m.||||||07-NOV-08
36851|Woodbrook Formation|23784|5|Briefly described|p10|Archean|Archean|Of Whundo Group.||||||07-NOV-08
36851|Woodbrook Formation|23789|5|Briefly described|p9 Tb. 2|Archean|Archean|Of the Whundo Group.  Max. thickness: 1000m.  Age: 3117+/-3Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
36851|Woodbrook Formation|23793|4|Described|p17|Archean|Archean|Of Whundo Group. See also page 11 table 2 Age: 3117+/-3Ma. Max. thickness: 1000m.||||||07-NOV-08
36851|Woodbrook Formation|23794|5|Briefly described|Map Legend|Archean|Archean|Of Whundo Group. Underlain by Bradley Basalt. Geological Province: Pilbara Craton.||||||07-NOV-08
36851|Woodbrook Formation|24023|5|Briefly described|p7 fig. 4|Archean|Archean|Of Whundo Group. Maximum thickness: 1000m.||||||07-NOV-08
36851|Woodbrook Formation|24184|4|Described|p712 Tb.5|Archean|Archean|Of the Whundo Group. Underlain by Bradley Basalt. Geological Province: Pilbara Craton. Max Thickness: 1000m. Age: 3117 +/- 3Ma (Nelson 1998).||||||07-NOV-08
36851|Woodbrook Formation|24353|4|Described|p11 Tb.2|Archean|Archean|Of the Whundo Group. Age: 3117 +/- 3Ma. Max Thickness: 1000m. Geological Province: Pilbara Craton||||||07-NOV-08
36851|Woodbrook Formation|24541|5|Briefly described|p12, p16 Tb.3|Archean|Archean|Of the Whundo Group. Age: rhyolite tuff dated at 3118+/-2 Ma (Nelson, 1998).||||||07-NOV-08
36851|Woodbrook Formation|24550|5|Briefly described|p36 Tb. 3.2|Archean|Archean|Of the Whundo Group. Basalt and felsic volcanics. Age: 3115Ma. Thickness: 1000m. Geological Province: Pilbara Craton.||||||07-FEB-11
36851|Woodbrook Formation|50430|5|Briefly described|p163||Archean|Felsic volcanics in Whundo Group.||||||07-NOV-08
36851|Woodbrook Formation|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Age: <3.10Ga. Geological Province: Pilbara Craton.||||||07-NOV-08
36851|Woodbrook Formation|63441|4|Described|p5 Tb.1, p24|Archean|Archean|Of Whundo Group (Pilbara Supergroup). Conformable over Bradley Basalt. Geol.prov: West Pilbara Superterrane. Consists of metamorphosed rhyolite tuff and agglomerate, and smaller amounts of metabasalt; rare units of carbonate-rich, ferruginous chert + BIF.||||||07-FEB-11
36851|Woodbrook Formation|63538|5|Briefly described|p6 Fig. 3|Archean|Archean|Of Whundo Group. Unconformably overlain by Cleaverville Formation. Underlain by Bradley Basalt. Geological Province: Pilbara Craton.||||||01-JUL-14
36851|Woodbrook Formation|64174|5|Briefly described|Map legend|Archean|Archean|Of the Whundo Group. Age: c.3117Ma. Rhyolitic tuff and agglomerate; minor basalt and rare banded iron formation; metamorphosed.||||||07-NOV-08
36851|Woodbrook Formation|64580|4|Described|map legend||Mesoarchean|Of Whundo Group. Rhyolite tuff and agglomerate; minor basalt and rare thin banded iron-formation; metamorphosed.||||||15-DEC-08
36851|Woodbrook Formation|64632|6|Mentioned|p203 Fig.2|||Of or overlying the Whundo Group.||||||
36851|Woodbrook Formation|67201|4|Described|p7 Fig.4, p12 Tb.1, p15-18, p49|Archean|Archean|In northwestern Pilbara Craton, West Pilbara Superterrane, Sholl Terrane, Whundo Basin.|c. 3118 Ma|Whundo Group||Conformably overlies Bradley Basalt. Is overlain by Mount Roe Basalt (high-angle angular erosional unconformity).|Felsic volcanics: rhyolitic tuff and agglomerate; minor basalt and rare thin banded iron formation; metamorphosed.|
36851|Woodbrook Formation|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological province: West Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 3117 Ma|Unit of Whundo Group.|||Rhyolite tuff and agglomerate; minor basalt and rare thin banded iron-formation; metamorphosed|
36851|Woodbrook Formation|69299|5|Briefly described|p6 Tb.1|Mesoarchean|Mesoarchean|Concealed on COOYA POOYA. Thickness on COOYA POOYA: 1000 m.|3117 +/- 3 Ma||||Rhyolite tuff and agglomerate, and minor basalt and thin banded iron-formation.|
36851|Woodbrook Formation|69300|5|Briefly described|map legend|Archean|Archean|West Pilbara Granite-Greenstone Terrane. Isotopic age: shown on legend as c. 3115 Ma|3117+/-3 and 3118+/-2 Ma isotopic age, Nelson 1998|Whundo Group|||Rhyolitic tuff and agglomerate; minor basalt and banded-iron formation; metamorphosed.|03-SEP-14
36851|Woodbrook Formation|69301|4|Described|p5 Fig.3, p9 Tb.1|||Pilbara Craton. West Pilbara Superterrane. Whundo Basin. Sholl Terrane.|3118 Ma|Whundo Group||Conformably overlies Bradley Basalt.|Felsic volcanic rocks. Comprises metamorphosed rhyolite tuff and agglomerate, and only minor metabasalt.|
36851|Woodbrook Formation|70022|6|Mentioned|p115|||West Pilbara Superterrane.||Whundo Group.||||
36851|Woodbrook Formation|70775|4|Described|p12, p15, p32, p33 fig 21, p36, p41|Mesoarchean||Whundo Basin. A type area is located west of Woodbrook and here it is 1000m thick. Dated at 3117 +/- 3 Ma (Nelson 1998c).|3115-3110 Ma|Whundo Group||Overlies the Bradley Basalt. Unconformably overlain by the Farrel Quartzite.|Rhyolitic tuff and agglomerate; minor basalt and rare thin banded iron-formation; metamorphosed.|
36851|Woodbrook Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Whundo Basin.|Max age 3115+/-5 Ma, min ~3110 Ma.|Whundo Group|||Rhyolite tuff and agglomerate; minor basalt and rare thin banded iron-formation; metamorphosed.|
36851|Woodbrook Formation|72251|5|Briefly described|p54|Mesoarchean|Mesoarchean|Geological province: West Pilbara Superterrane, Pilbara Craton.||||Overlain by Cleaverville Formation. Underlain by Bradley Basalt.||
36851|Woodbrook Formation|72668|6|Mentioned|p4, p12|||West Pilbara Superterrane.||Whundo Group||Overlies the Bradley Basalt.||
36834|Woodiana Member|23570|6|Mentioned|p129|||Equivalent of the Woodiana Sandstone Member and Woodiana Sandstone.   Underlain by the Mount Jope Volcanics. Max. thickness: 60m.  Geological Province: Pilbara Craton.||||||07-APR-09
36834|Woodiana Member|23575|5|Briefly described|Map Legend|Archean|Archean|Of Jeerinah Formation. Overlying unit Isabella Member. Underlying unit Maddina Formation.||||||07-NOV-08
36834|Woodiana Member|24533|5|Briefly described|p11|Archean|Archean|Of the Jeerinah Formation. Comprises quartz rich sandstone interbedded with subordinate chert, chert breccia, mudstone and volcanogenic lithic sandstone. Conformably overlies the Maddina Formation. Geological Province: Hamersley Basin.||||||07-NOV-08
36834|Woodiana Member|24534|5|Briefly described|Map legend|Archean|Archean|Of the Jeerinah Formation.  Quartz-rich sandstone, chert, chert breccia and mudstone.  Age: c.2717Ma.  Geological Province: Hamersley Basin.||||||07-NOV-08
36834|Woodiana Member|50131|6|Mentioned|p6 Fig. 4|||Of Fortescue Group. Geological Province: Pilbara Craton.||||||22-APR-09
36834|Woodiana Member|60373|6|Mentioned|p162|||Of Thorne and Tyler, 1996. Of Jeerinah Formation.||||||
36834|Woodiana Member|62129|3|Fully described|p8|Archaean|Archaean|Of Jeerinah Formation. Max thickness: 50m. Geological Province: Hamersley Basin. Cross-stratified quartz sandstone, with minor pelite and chert. Interpreted as a transgressive shoreline deposit.||||||07-FEB-11
36834|Woodiana Member|62130|5|Briefly described|Map Legend|Archaean|Archaean|Of Jeerinah Formation. Geological Province: Hamersley Basin, Pilbara Craton. Metamorphosed quartzitic sandstone, pelite, and chert.||||||23-DEC-09
36834|Woodiana Member|62579|5|Briefly described|p116|Archean|Archean|Basal unit of Jeerinah Formation (Fortescue Group, Mount Bruce Supergroup). Overlies Maddina Basalt. Geological Province: Pilbara Craton. Contains stromatolites.||||||07-NOV-08
36834|Woodiana Member|63372|4|Described|Map Legend|Archean|Archean|Of the Jeerinah Formation. Geological Province: Hamersley Basin. Quartz rich sandstone, chert, chert breccia, and mudstone, locally includes lithic volcaniclastic sandstone. Overlies the Maddina Formation.||||||07-NOV-08
36834|Woodiana Member|66685|5|Briefly described|p217 Fig.2|Archean|Archean|||Jeerinah Formation||Underlies the Warrie Member.|Sandstone with stromatolites.|
36834|Woodiana Member|67201|5|Briefly described|p29 Fig.15, p32, p51|||Northern Fortescue Basin, Northeast and Northwest Pilbara Sub-basins. Lower section of nearshore shelf deposits up to 60 m thick.||Jeerinah Formation||||25-NOV-16
36834|Woodiana Member|69301|4|Described|p18 Fig.7, p19, p22|||Pilbara Craton. Fortescue Basin. Northeast Pilbara Sub-basin, Northwest Pilbara Sub-basin, Sequence 4. Thickness: up to 60 m.||Base of Jeerinah Formation|||Consists of near-shore facies sandstone with local deposits of silicified stromatolitic limestone.|
76752|Woodlands Member (WA)|67245|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Edmund Basin.||Unit in Irregully Formation.|||Thick-bedded quartz sandstone; minor siltstone.|02-FEB-12
68661|Woodline Formation|24165|5|Briefly described|Plate 1|Mesoproterozoic|Paleoproterozoic||||||Arenaceous and argillaceous metasedimentary rocks, including silicified evaporite.|
68661|Woodline Formation|50011|5|Briefly described|p60, 62 Fig. 2|Proterozoic|Proterozoic|Quartz arenite, quartz conglomerate, argillite, mudstone; weakly deformed, with gentle upright folding and warping; weakly to moderately developed subvertical cleavage. Age: 1620 +/- 100Ma. Geological Province: Albany-Fraser Orogen. Of Biranup Complex.||||||12-OCT-06
68661|Woodline Formation|60555|4|Described|p2 Fig. 1, p4 Tb. 1, p13, p16-18, p20|Proterozoic|Proterozoic|Formerly Woodline beds; Griffin, 1989. Age of deposition: <1620Ma and 1620+/-100Ma (Rb-Sr, Turek, 1966). Thickness: 250m. NW to SE paleoflow direction. Consists of quartz-rich sandstone and interbedded siltstone with minor clast-supported conglomerate.||||||01-MAY-13
68661|Woodline Formation|62093|5|Briefly described|p214 Fig. 1, p223|Proterozoic|Proterozoic|Quartz arenite. Age: <1600+/-100Ma. Max. deposition age: 1737Ma (detrital zircons).||||||
68661|Woodline Formation|63866|4|Described|p184-p185, p193|Proterozoic|Proterozoic|Northern Foreland. SHRIMP age is interpreted as the maximum depositional age for this formation and is derived from six samples of coarse-grained quartz sandstone dated at: 2004 +/- 27 Ma, 2003 +/- 50 Ma, 1886 +/- 13 Ma, 1884 +/- 21, 1880 +/- 17 Ma and 1737 +/- 28 Ma.|c. 1737 Ma (SHRIMP U-Pb)||||Quartz sandstone, quartz conglomerate, chert breccia and interlayered mudstone.|
68661|Woodline Formation|64161|3|Fully described|p577-595|Statherian|Statherian|Unconformably overlies Eastern Goldfields Superterrane. Formerly: Woodline Beds. Max depositional SHRIMP age of 1737+/-28 Ma. Minimum depositional age: 1345 Ma (Albany -Fraser Orogeny initiation)|||||Fluvial to fluvial-marine succession, mainly sandstone.|21-MAR-12
68661|Woodline Formation|64340|4|Described|p2 Fig. 1, p5 Fig. 3, p7, p23-25|Proterozoic|Proterozoic|Originally named Woodline Beds by Sofoulis and Bock (1963). Age of deposition: 1737 - 1620Ma. Overlies Archaean basement. Thick: 250m. Consists of mainly quartz-rich sandstone and minor conglomerate and siltstone. See p23-24 for detailed info.||||||08-FEB-10
68661|Woodline Formation|64577|6|Mentioned|p607, p616|||Age: 1800-1700Ma.||||||
68661|Woodline Formation|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Quartz sandstone, quartz conglomerate, and mudstone.||||||15-DEC-08
68661|Woodline Formation|64635|6|Mentioned|p2 Fig.1|||||||||
68661|Woodline Formation|64730|6|Mentioned|p138|Paleoproterozoic|Paleoproterozoic|SE margin of Yilgarn Craton. Includes detrital zircons of 2035 Ma (Hall & Jones 2005).||||||03-MAY-12
68661|Woodline Formation|65257|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Quartz sandstone, quartz conglomerate, and mudstone.||||||
68661|Woodline Formation|65260|5|Briefly described|p6 Tb.1, p7, p8 Fig.3, p14-15, p20|Calymmian|Statherian|1620+/-100 Ma. Formerly Woodline Beds (Griffin 1989). c. 250 m thick. Quartz arenite, siltstone, and minor quartz conglomerate and mudstone; in places chert breccias are interbedded with finer-grained quartz-rich sst, minor chert and mudstones; unconformably overlies Archean rocks. Only weakly deformed (greenschist metamorphism): sedimentary structures preserved. May be a lateral equivalent of Mount Barren Group.||||||01-JUL-14
68661|Woodline Formation|65487|6|Mentioned|p2 Fig.1, p24, p57 Fig 28|Paleoproterozoic|Paleoproterozoic|Found 350 km NE of the Mount Barren Group. Consists of lower greenschist facies mature sandstone interbedded with siltstone. Detrital zircon age spectra similar to Earaheedy Group; maximum depositional age 1737 +/- 28 Ma.||||||
68661|Woodline Formation|67268|6|Mentioned|p4|||||||||
68661|Woodline Formation|67380|6|Mentioned|p6 Fig.3, p15 Fig.14|||Albany-Fraser Orogen.||||||
68661|Woodline Formation|67722|6|Mentioned|p5 fig 2.2|||||||||
68661|Woodline Formation|68186|5|Briefly described|p3 Fig.2, p8, p11, p13-15, p39, p80|Paleoproterozoic|Paleoproterozoic|See also Plate 1A. Northern Foreland, Albany-Fraser Orogen. Assigned to the newly-named Barren Basin, overlying the Yilgarn Craton. Detrital zircon age spectra are most similar to the upper Earaheedy Group on NE Yilgarn Craton. Plate 1A give an age of c.1750 Ma.|<1737 +/- 28 Ma (maximum depositional age).||||Weakly deformed, lower greenschist facies, mature sandstone interbedded with siltstone. Minor units of pebble and cobble conglomerates, and matrix- to clast-supported chert breccias.|
68661|Woodline Formation|68654|6|Mentioned|p3, p2 Fig 2|Paleoproterozoic|Paleoproterozoic|Barren Basin.||||||
68661|Woodline Formation|69003|5|Briefly described|vi, p28, p30, p72|||Barren Basin. Siliciclastic sediments, deposited on the S Yilgarn Craton after c.1800 Ma. Geochronology (U-Pb and diagenetic xenotime) described. Maximum depositional age.|< c.1737 Ma.||||Dominantly shallow-marine to fluvial, mature, quartz-rich sandstones with interbedded siltstones and minor conglomerate.|
68661|Woodline Formation|69140|6|Mentioned|p2-3|||Geological province: Albany-Fraser Orogen.||||||
68661|Woodline Formation|69152|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Sandstones ~10, 40m above base dated with maximum depostional age 1737+/- 28 Ma,  1880+/-17 Ma, 1886+/-13 Ma U/Pb SHRIMP. See geochron file 165593.1.pdf, 165591.1.pdf, 165592.1.pdf,179097.1.pdf, 179098.1.pdf, 179602.1.pdf (2006).|Max. depostional age 1737+/- 28 Ma||Includes 5 unnamed subunits.||Quartz sandstone, quartz conglomerate, siltstone and mudstone.|07-AUG-15
68661|Woodline Formation|69252|5|Briefly described|p7 Fig.3, p9, p12|||Albany-Fraser Orogen. Forms a 50km-long, NE-trending belt of quartz-rich metasedimentary rocks cropping out as heavily vegetated low hills. Over 250m thick.|||||Mature, quartz-rich sandstone units interbedded with siltstones; minor chert breccia and pebble-cobble conglomerates.|
68661|Woodline Formation|69386|5|Briefly described|p4, p6, p37|Proterozoic|Archean|Biranup Zone, Albany-Fraser Orogen. Remnants of the 1.8 to 1.6 Ga Barren Basin.|||||Metamorphosed quartz sandstone, mudstone and conglomerate.|
68661|Woodline Formation|69595|5|Briefly described|p3 fig 1, p8, p10 tbl 2, p12,|Statherian|Rhyacian|Yilgarn Craton, Barren Basin, Woodline Sub-basin. Deposited in a distal-fluvial to marine environment.Paleocurrent directions are recorded as southeasterly to southwesterly. Significant portions of this unit are made up of c. 1800 Ma detritus. At least 250m thick.  Other significant age components are mentioned [see page 18]. See also  p13 fig 7a, p15, p16 tbl 3, p18, p19, p35, p38, p39 fig 22, p40, p57.|2246 - 1651 +/- 26 Ma|||Possible lateral equivalent of the Earaheedy Group.|Quartz-rich sandstone interbedded with thicker horizons of siltstone. Pebbly conglomerate, quartzite and thinly bedded siltstone also occurs.|
68661|Woodline Formation|70017|6|Mentioned|p223|Mesoproterozoic|Mesoproterozoic|SE Yilgarn Craton. Overlies basement. Open upright NE-oriented folds produced during the Albany-Fraser orogeny.|<1737 Ma (Hall and Jones, 2005).||||Lower greenschist facies metamorphism.|
68661|Woodline Formation|70023|6|Mentioned|p167|||Albany-Fraser Orogen.||||||
68661|Woodline Formation|70084|6|Mentioned|p219|||Geological province: Yilgarn Craton.||||||
68661|Woodline Formation|70085|6|Mentioned|p234 Fig.1|||Albany-Fraser Orogen.||||||
68661|Woodline Formation|70089|6|Mentioned|p262|||Albany-Fraser Orogen.||||||
68661|Woodline Formation|70090|4|Described|p442,444,446-447,453,457-459|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen, West Australian Craton. Of Woodline Sub-basin, Barren Basin. Thickness: >250m. Deposited in a broad, relatively shallow basin under moderate to high-energy, fluvial to shallow marine environments. Deposition occurred in the late stages of, or shortly after, Biranup Orogeny.  Inversion related to Zanthus Event (of Biranup orogeny) may had eroded and shed detritus into Barren Basin. Metamorphosed to greenschist facies. Maximum depositional age: c.1696 Ma. Minimum depositional age: contrained by Stage I and/or Stage II AFO deformation (Hall et al., 2008).  Detrital zircon Paleoproterozoic age components include c. 2475, 2457, 2292, 2246, 2035, 1988, 1883, 1794, and 1696 Ma. Archean age components include c. 2838, 2795, 2687, 2665, 2652, 2629, 2570, and 2528 Ma.|||||Quartz-rich sandstone, pebbly conglomerate, siltstone.|
68661|Woodline Formation|70153|5|Briefly described|100k_geologyp10_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop14_lut.csv. Woodline Sub-basin, Barren Basin. Age (derived from samples of quartz sandstone and metasandstone) of 2672 +/- 6 Ma (SHRIMP) represents maximum age of protolith deposition (165593.1.pdf, 183145.1.pdf).|1737 +/- 28 Ma (isotopic) - 1700 Ma (inferred).||||Quartz sandstone, quartz conglomerate, mudstone, shale, siltstone, sedimentary breccia and breccia composed of angular clasts.|
68661|Woodline Formation|70182|6|Mentioned|p3-5|Paleoproterozoic|Paleoproterozoic|Woodline Sub-basin, Albany-Fraser Orogen.||||||
68661|Woodline Formation|70256|6|Mentioned|p3|||Albany-Fraser Orogen.||||||
68661|Woodline Formation|70795|6|Mentioned|Intro_2004.pdf|||||||||
68661|Woodline Formation|70802|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Geological province: Albany-Fraser Orogen. Of Barren Basin. Events: Albany-Fraser Orogeny Stage II (1225-1140 Ma); Albany-Fraser Orogeny (1330-1140 Ma); Albany-Fraser Orogeny Stage I (1330-1260 Ma); Biranup Orogeny (1710-1620 Ma). Samples GSWA 165591 and 165591 (quartz sandstones; same stratigraphic layer) yielded weighted mean 207Pb*/206Pb* dates of 1880+\-17 Ma and 1886+\-13 Ma respectively, interpreted to be maximum depositional age of the quartz sandstone samples. Sample GSWA 165593 (quartz sandstone; near base of Woodline formation) yielded a weighted mean 207Pb*/206Pb* date of 1737+\-28 Ma, interpreted to be maximum depositional age of the quartz sandstone. Sample GSWA 179097 (quartz sandstone; base of Woodline formation) yielded a weighted mean 207Pb*/206Pb* date of 2004+\-27 Ma, interpreted to be maximum depositional age of the quartz sandstone. Sample GSWA 179098 (quartz sandstone) yielded a weighted mean 207Pb*/206Pb* date of 1884+\-21 Ma, interpreted to be maximum depositional age of the quartz sandstone. Sample GSWA 179602 (quartz sandstone) yielded a weighted mean 207Pb*/206Pb* date of 2003+\-50 Ma, interpreted to be maximum depositional age of the quartz sandstone. See 500k_interpgeop14_lut.csv, 250k_pre_mesozoic_interpgeop_lut.csv, 100k_geologysub10_lut.csv.|1734+\-28 Ma; 1700 Ma (inferred)||||Intercalated layers of quartz sandstone, quartz conglomerate, and mudstone; metamorphosed|
68661|Woodline Formation|70826|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|Southeastern margin of Yilgarn Craton.||||||15-MAY-20
68661|Woodline Formation|70858|6|Mentioned|p32 Figs.15C-D, p33|Paleoproterozoic|Paleoproterozoic|||||||
68661|Woodline Formation|71168|5|Briefly described|p36|||Yilgarn Craton.|||||Quartz sandstone with minor conglomerate.|
68661|Woodline Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, conglomerate, mudstone, shale|
68661|Woodline Formation|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Albany-Fraser Orogen, West Australian Craton. Of Barren Basin. Events: Albany-Fraser Orogeny Stage II (1225 - 1140 Ma); Albany-Fraser Orogeny (1330 - 1140 Ma); Albany-Fraser Orogeny Stage I (1330 - 1260 Ma); Biranup Orogeny (1710 - 1620 Ma). Sample GSWA 165591 (quartz sandstone; 40m from stratigraphic base of Woodline Formation) yielded weighted mean 207Pb/206Pb date of 1880+\-17 Ma, interpreted as maximum depositional age of the sandstone. Sample GSWA 165592 (quartz sandstone; 40m from stratigraphic base of Woodline Formation) yielded weighted mean 207Pb/206Pb date of 1886+\-13 Ma, interpreted as maximum depositional age of the sandstone. Sample GSWA 165593 (quartz sandstone; 10m from stratigraphic base of Woodline Formation) yielded weighted mean 207Pb/206Pb date of 1737+\-28 Ma, interpreted as maximum depositional age of the sandstone. Samples GSWA 179097 and 179098 (both are coarse grained quartz sandstone) yielded weighted mean 207Pb/206Pb date of 2004+\-7 Ma and 1884+\-21 Ma respectively, interpreted to be maximum depositional ages of the sandstone samples. Sample GSWA 179602 (quartz sandstone) yielded a weighted mean 207Pb/206Pb date of 2003+\-50, interpreted to be maxumum depositional age of the sandstone.  See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv1m_geologyp12_lut.csv, 100k_geologysub10_lut.csv, 2_5m_interpgeop15_lut.csv.|1651+\-26 Ma; 1600 Ma (inferred)||||Quartz sandstone, quartz conglomerate, mudstone, shale, siltstone, minor conglomerate, sedimentary breccia; angular quartz clasts.|
68661|Woodline Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Woodline Sub-basin, Barren Basin.|Max age 1651+/-26 Ma,  Min ~1600 Ma.||||Quartz sandstone, quartz conglomerate, and mudstone; metamorphosed.|
68661|Woodline Formation|72059|6|Mentioned|p56|Mesoproterozoic|Mesoproterozoic|Geological province: Fraser Zone, Albany-Fraser Orogen.||||||
68661|Woodline Formation|72710|6|Mentioned|p4 Fig.2.|Paleoproterozoic|Paleoproterozoic|Shown as WF on p4 Fig.2. Shown as part of the Barren Basin.|1600 Ma to 1815 Ma.|||||
68661|Woodline Formation|73084|6|Mentioned|p12|||Yilgarn Craton.||||||
68661|Woodline Formation|73238|6|Mentioned|p22|Proterozoic|Proterozoic|Kurnalpi Terrane.||||||
25647|Woodrarrung Sandstone|23569|6|Mentioned|p7|Proterozoic|Proterozoic|Superseded by Woodrarrung Formation||||||
25647|Woodrarrung Sandstone|29690|5|Briefly described|p13|||||||||
25647|Woodrarrung Sandstone|36199|6|Mentioned|p1|||||||||
25647|Woodrarrung Sandstone|36293|6|Mentioned|p77|||||||||
25647|Woodrarrung Sandstone|36872|4|Described|p71|||||||||
25647|Woodrarrung Sandstone|37460|5|Briefly described|p177|||||||||
25647|Woodrarrung Sandstone|38494|4|Described|p25|||||||||
25647|Woodrarrung Sandstone|38998|4|Described|p12|||||||||
25647|Woodrarrung Sandstone|40336|5|Briefly described|p15|||||||||
25647|Woodrarrung Sandstone|40340|5|Briefly described|p7|||||||||
25647|Woodrarrung Sandstone|40341|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Middle to Late||||||
25647|Woodrarrung Sandstone|40342|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Middle to Late||||||
25647|Woodrarrung Sandstone|40343|5|Briefly described|p3|||||||||
25647|Woodrarrung Sandstone|44142|5|Briefly described|p328 Tb. 4-5|||||Badgeradda Group|||Feldspathic and quartz sandstone.|
25647|Woodrarrung Sandstone|45015|3|Fully described|p21-22, map legend|Proterozoic|Proterozoic|Of Badgeradda Group. Lower medium- to coarse-grained sandstone and upper fine- to medium-grained kaolinitic sandstone. Conformable overlaps Bililly Formation; conformably underlies Coomberarie Formation. Max. thickness: 3700ft. Geol.Prov: Carnarvon Basin.||||||31-MAY-06
25647|Woodrarrung Sandstone|48823|3|Fully described|p11, map legend, p10 Tb. 2|Paleoproterozoic|Paleoproterozoic|Of the Badgeradda Group. Light grey to white, x-stratified, thick bedded, medium to coarse quartz sandstone and thin bedded, fine- to medium-gr. kaolinitic sandstone. Conformable over Bililly Fm; conformably underlies Coomberarie Fm. Thickness: >1625ft.||||||07-NOV-08
25647|Woodrarrung Sandstone|61958|5|Briefly described|Map sheet 1|Neoproterozoic|Neoproterozoic|Of the Badgeradda Group.||||||21-MAR-06
25647|Woodrarrung Sandstone|69583|5|Briefly described|p130, p133, p156, Plate 3|Proterozoic|Proterozoic|Badgeradda Basin. Is inferred to continue subsurface to the N, beneath the Byro Sub-basin of the Southern Carnarvon Basin.|c.1080 Ma (maximum depositional age).|Badgeradda Group.|||Medium- to coarse-grained quartzose sandstone, commonly silicified; overlain by fine- to medium-grained feldspathic sandstone.|
25647|Woodrarrung Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
25647|Woodrarrung Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Neoproterozoic|Neoproterozoic|Badgeradda Basin.||Badgeradda Group|||Medium- to coarse-grained quartzose sandstone, commonly silicified, overlain by fine- to medium-grained feldspathic sandstone.|
36960|Woodstock Monzogranite|23416|5|Briefly described|Map Legend|Archean|Archean|Of Yule Granitoid Complex, Pilbara Craton||||||07-NOV-08
36960|Woodstock Monzogranite|23755|5|Briefly described|p54|Archean|Archean|See also page 18 Table 2. Geological Province: Yule Granitoid Complex.||||||07-NOV-08
36960|Woodstock Monzogranite|24531|5|Briefly described|p8-9 Fig. 3|Archean|Archean|Of the Yule Granitoid Complex.  Age: 2933+/-3Ma.  See also p25 Fig. 10||||||07-NOV-08
36960|Woodstock Monzogranite|24532|5|Briefly described|Map legend|Archean|Archean|Age: 2933-2927Ma.  Of the Yule Granitoid Complex.||||||07-NOV-08
36960|Woodstock Monzogranite|24554|4|Described|p5 Tb.1, p8|Archean|Archean|Of the Yule Granitoid Complex. Age: 2933 +/- 3 Ma (Nelson, 1998). Geological Province: East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
36960|Woodstock Monzogranite|50146|5|Briefly described|Map Legend|Archean|Archean|Of the Yule Granitoid Complex. Age: c. 2933-2927 Ma. Geological Province: Pilbara Craton. Equigranular to feldspar-porphyritic biotite monzogranite; weakly to moderately foliated; locally abundant pegmatite and granodiorite dykes.||||||07-NOV-08
36960|Woodstock Monzogranite|50379|5|Briefly described|Map Legend|Archean|Archean|Of Yule Granitoid Complex. Geological Province: Pilbara Craton. Age: c. 2925 Ma||||||07-NOV-08
36960|Woodstock Monzogranite|61252|6|Mentioned|p67 Tb.1|||Of the Yule granitoid complex.||||||
36960|Woodstock Monzogranite|63441|5|Briefly described|p11 Tb. 2|Archean|Archean|Of Sisters Supersuite. Geological province: Pilbara Craton.||||||07-FEB-11
36960|Woodstock Monzogranite|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Unit in Sisters Supersuite. 2933-2927 Ma. Biotite monzogranite; equigranular to feldspar-porphyritic; weakly to moderately foliated; locally abundant pegmatite and granodiorite dykes; magnetite-bearing leucogranite pods.||||||
36960|Woodstock Monzogranite|68282|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|c.2933 Ma; c.2927 Ma.|Of the Sisters Supersuite|||Biotite monzogranite, equigranular to feldspar porphyritic, weakly to moderately foliated, locally abundant pegmatite and granodiorite dykes, magnetite-bearing leucogranite pods; local rafts and inclusions of Petroglyph Gneiss; local mafic layering.|
36960|Woodstock Monzogranite|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|2933-2927 Ma|Of the Sisters Supersuite.|||Biotite monzogranite; equigranular to feldspar-porphyritic; weakly to moderately foliated; locally abundant pegmatite and granodiorite dykes;  magnetite-bearing leucogranite pods.|30-APR-14
36960|Woodstock Monzogranite|69015|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|2933-2927 Ma|Of the Sisters Supersuite.|||Biotite monzogranite, equigranular to feldspar porphyritic, weakly to moderately foliated; with locally abundant pegmatite and granodiorite dykes and magnetite-bearing leucogranite pods, or with abundant greenstone and granitic gneiss xenoliths.|02-MAY-14
36960|Woodstock Monzogranite|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Sisters Supersuite|||Biotite monzogranite; weakly to moderately foliated; locally abundant pegmatite and granodiorite dykes; magnetite-bearing leucogranite pods K-feldspar-porphyritic monzogranite, biotite monzogranite with mafic layering and schlieren.|
36960|Woodstock Monzogranite|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; North Pilbara Orogeny. See 100k_geologyp_lut.csv, 500k_interpgeop_lut.csv.|2933-2927 Ma (isotopic, inferred)|Unit of Sisters Supersuite.|||Biotite monzogranite, K-feldspar-porphyritic monzogranite with common rafts and inclusions of tonalitic orthogneiss (Petroglyph Gneiss).|
36960|Woodstock Monzogranite|71137|6|Mentioned|p3|Archean|Archean|Pilbara.|2927 +/- 3 Ma (SHRIMP: van Kranendonk, 2010).|||Intrudes Lalla Rookh Formation.||
36960|Woodstock Monzogranite|71267|4|Described|GEOL_LUT_CSV files||||||||monzogranite, pegmatite, felsic gneiss|
36960|Woodstock Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||Max age 2933+/-3 Ma, Min  2927+/-3 Ma.|Sisters Supersuite|||Biotite monzogranite; equigranular to feldspar porphyritic; weakly to moderately foliated; locally abundant pegmatite and granodiorite dykes; magnetite-bearing leucogranite pods.|
27939|Woodward Dolerite|22496|3|Fully described|p8||Orosirian|Some areas previously mapped as Woodward Dolerite (Gemuts and Smith, 1968) are now considered to be thick basaltic flows within the Biscay Formation. Geological province: Halls Creek Province.||||||05-FEB-08
27939|Woodward Dolerite|22526|6|Mentioned|Fig3 P682||Orosirian|||||||
27939|Woodward Dolerite|22547|6|Mentioned|p9|||||||||
27939|Woodward Dolerite|22754|5|Briefly described|p3||Paleoproterozoic|In the Lamboo Complex. Intrudes the Olympio and Biscay Formations.  Max. thickness: 200m.||||||07-NOV-08
27939|Woodward Dolerite|22764|4|Described|Table1,p7||Paleoproterozoic|||||||01-FEB-10
27939|Woodward Dolerite|22777|5|Briefly described|Map|||||||||
27939|Woodward Dolerite|23205|6|Mentioned|p42|Paleoproterozoic|Paleoproterozoic|In the Halls Creek Inlier.||||||07-NOV-08
27939|Woodward Dolerite|23383|6|Mentioned|p12|||Extensive mafic sills that intrude Halls Creek Group.||||||25-JAN-05
27939|Woodward Dolerite|23599|4|Described|p10|Paleoproterozoic|Paleoproterozoic|Geological Province: Lamboo Complex.||||||07-NOV-08
27939|Woodward Dolerite|23621|4|Described|p17|Paleoproterozoic|Paleoproterozoic|See also page 11 table 1. Age: 1910-1850 Ma. Geological Province: Halls Creek Orogen. Max. thickness: 200 m.||||||07-NOV-08
27939|Woodward Dolerite|23622|5|Briefly described|Map Legend|Orosirian||Age: >1880-1847 Ma.||||||
27939|Woodward Dolerite|23722|6|Mentioned|p8|||Not a current name - renamed Ruins Dolerite||||||
27939|Woodward Dolerite|24173|4|Described|p18|Paleoproterozoic|Paleoproterozoic|Formerly grouped with Bow River Batholith into Lamboo Complex. Max Thickness: 200m. Age: c.1880Ma.  Intruded Ding Dong Downs Volcanics and Halls Creek Group. Some outcrops now reinterpreted as lava flows. Geological Province: Halls Creek Orogen.||||||07-NOV-08
27939|Woodward Dolerite|24197|6|Mentioned|p132|||High Mg-tholeiite in the Kimberleys.||||||07-FEB-11
27939|Woodward Dolerite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|In the Lamboo Complex.  Fine- to medium-grained metadolerite.  Age: c.1840Ma.||||||07-NOV-08
27939|Woodward Dolerite|30525|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27939|Woodward Dolerite|30533|4|Described|p12|||On Table 1||||||
27939|Woodward Dolerite|30892|5|Briefly described|p96|||||||||
27939|Woodward Dolerite|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27939|Woodward Dolerite|30896|4|Described|p12|||Lower Proterozoic||||||
27939|Woodward Dolerite|30897|4|Described|p9|||See also p8.||||||14-NOV-06
27939|Woodward Dolerite|30898|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27939|Woodward Dolerite|31226|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27939|Woodward Dolerite|32728|5|Briefly described|p22|||Mention Fig.3||||||
27939|Woodward Dolerite|34684|6|Mentioned|p102|||||||||
27939|Woodward Dolerite|35120|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27939|Woodward Dolerite|36551|6|Mentioned|Table 14|||||||||14-NOV-06
27939|Woodward Dolerite|36885|5|Briefly described|p167|||Formerly McClintock Greenstones.||||||
27939|Woodward Dolerite|37462|4|Described|Table 4.I|||||||||
27939|Woodward Dolerite|41158|6|Mentioned|p146|||||||||
27939|Woodward Dolerite|41465|6|Mentioned|p6|||||||||
27939|Woodward Dolerite|41594|5|Briefly described|p72|||||||||
27939|Woodward Dolerite|41976|6|Mentioned|p453|||||||||
27939|Woodward Dolerite|41980|6|Mentioned|Fig.5 P587|||||||||
27939|Woodward Dolerite|41987|6|Mentioned|Fig.3 P73|||||||||
27939|Woodward Dolerite|42149|6|Mentioned|p703|||||||||
27939|Woodward Dolerite|42326|5|Briefly described|p9|||||||||
27939|Woodward Dolerite|42329|4|Described|p5|||See also Fig.2 p6 and p19.||||||14-NOV-06
27939|Woodward Dolerite|42757|6|Mentioned|p10|||||||||
27939|Woodward Dolerite|42811|5|Briefly described|p6|||Of Halls Creek Group.||||||14-NOV-06
27939|Woodward Dolerite|42814|6|Mentioned|p6|||||||||
27939|Woodward Dolerite|43299|5|Briefly described|Map Legend||Paleoproterozoic|Of the Duerdin Group.||||||07-NOV-08
27939|Woodward Dolerite|43303|5|Briefly described|Map Legend||Paleoproterozoic|Of the Birrindudu Group.||||||07-NOV-08
27939|Woodward Dolerite|43632|6|Mentioned|p2||Proterozoic|||||||
27939|Woodward Dolerite|43666|6|Mentioned|p52,Table 2||Neoproterozoic|||||||
27939|Woodward Dolerite|43854|5|Briefly described|Map Legend||Proterozoic|||||||
27939|Woodward Dolerite|44155|4|Described|p234-235,p238,p248 Tb.3-8,p254 Fig.3-40|Paleoproterozoic|Paleoproterozoic|Has chemical affinities with modern MORB.||Lamboo Complex.||Intrudes Biscay and Olympio Formations.|Dykes and sills of uralitized dolerite.|
27939|Woodward Dolerite|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Fine- to medium-grained metadolerite. In the Lamboo Complex (eastern zone).||||||07-NOV-08
27939|Woodward Dolerite|44317|5|Briefly described|Table 1||Proterozoic|||||||
27939|Woodward Dolerite|44318|14|Not recorded|map legend||Proterozoic|Proterozoic.||||||
27939|Woodward Dolerite|44324|14|Not recorded|p.7||Proterozoic|Tb.1, see page 5. (Proterozoic).||||||
27939|Woodward Dolerite|44325|14|Not recorded|map legend||Proterozoic|Proterzoic. Submitted Defn. on Tech.File SE/52-10.||||||
27939|Woodward Dolerite|44397|14|Not recorded|p.8, Table 1||Proterozoic|In the Lamboo Complex.||||||14-NOV-06
27939|Woodward Dolerite|44398|14|Not recorded|map legend||Proterozoic|||||||
27939|Woodward Dolerite|44693|5|Briefly described|Map Legend||Proterozoic|||||||
27939|Woodward Dolerite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
27939|Woodward Dolerite|45047|5|Briefly described|p13|||See also ppP17-18.||||||14-NOV-06
27939|Woodward Dolerite|45048|4|Described|p12|||Archaean or L. Proterozoic. p13.||||||14-NOV-06
27939|Woodward Dolerite|45087|5|Briefly described|p75|||See also p196. Chemical analyses.||||||14-NOV-06
27939|Woodward Dolerite|48931|3|Fully described|p16|||||||||
27939|Woodward Dolerite|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|In the Lamboo Complex (Eastern Zone). Medium to coarse grained metadolerite.||||||19-MAY-15
27939|Woodward Dolerite|60724|4|Described|p9, p5 Fig. 2|Paleoproterozoic|Paleoproterozoic|Parts previously mapped as Biscay Formation (Halls Creek Group). Thin dolerite sills however do intrude the Bisacay and Olympio Formations. Age: 1.85Ga (SHRIMP). Within the Lamboo Complex.||||||07-NOV-08
27939|Woodward Dolerite|61861|5|Briefly described|p15, Fig.2.|||Halls Creek Orogen. Correlated with older sills in Tanami Region.|c.1845 Ma.|||||
27939|Woodward Dolerite|62580|6|Mentioned|p71|||In the Halls Creek Orogen.||||||07-FEB-11
27939|Woodward Dolerite|63866|5|Briefly described|p130|||||||Intrudes the Halls Creek Group and the Ding Dong Downs Volcanics.||
27939|Woodward Dolerite|64104|6|Mentioned|p77|||Limited exposure in the core of the Osmond Range.||||||
27939|Woodward Dolerite|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Fine- to medium-grained metadolerite.||||||15-DEC-08
27939|Woodward Dolerite|65413|6|Mentioned|p105 Fig.1.|Paleoproterozoic|Paleoproterozoic|||Unit in Lamboo Complex.||||
27939|Woodward Dolerite|66846|6|Mentioned|p549 Fig.2|Orosirian|Orosirian|In the Eastern Zone of the Lamboo Complex.|||||Dolerite sills.|
27939|Woodward Dolerite|68078|6|Mentioned|p7 figure 4|Paleoproterozoic|Paleoproterozoic||~1855 Ma||||Dolerite.|
27939|Woodward Dolerite|68656|6|Mentioned|GEOL_LUT_CSV/500k_geologyp08_lut|Paleoproterozoic|Paleoproterozoic||||||Fine- to medium-grained metadolerite.|
27939|Woodward Dolerite|69003|6|Mentioned|p5, p19|||E zone, Lamboo Province, Halls Creek Orogen.||||||
27939|Woodward Dolerite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.|||||Fine- to coarse-grained metadolerite, and minor amphibolite.|04-AUG-15
27939|Woodward Dolerite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Fine- to coarse-grained metadolerite, and minor amphibolite.|
27939|Woodward Dolerite|69585|6|Mentioned|p4|||Eastern Lamboo Province.||||||
27939|Woodward Dolerite|69587|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Fine- to medium-grained metadolerite|
27939|Woodward Dolerite|69597|6|Mentioned|p5 fig 2b|||||||||
27939|Woodward Dolerite|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|1847-1808 Ma (Inferred)||||Fine- to coarse-grained metadolerite, and minor amphibolite|
27939|Woodward Dolerite|70154|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv.|1863-1865 Ma||||Fine to coarse grained metadolerite and minor amphibolite|
27939|Woodward Dolerite|70731|6|Mentioned|p268-269|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.||||||
27939|Woodward Dolerite|70812|5|Briefly described|p5-p6, p27|Orosirian||Eastern Zone of the Halls Creek Orogen, Lamboo Province.|<1850 Ma|||Intrudes the Halls Creek Group.||
27939|Woodward Dolerite|70851|5|Briefly described|p3-p4, p24|Paleoproterozoic|Paleoproterozoic|Eastern Zone, Lamboo Province.|c. 1850 Ma|||Intrudes the Halls Creek Group.||
27939|Woodward Dolerite|71113|5|Briefly described|p96,98|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen. Dolerite sills intruded into Halls Creek Group c. 1855 Ma during period of relaxation and local extension (Occhipinti et al., 2016).|c. 1855 Ma||||Dolerite sills.|
27939|Woodward Dolerite|71140|6|Mentioned|p96, 98|Orosirian|Orosirian|Eastern Zone, Lamboo Province, Halls Creek Orogen.|c.1855 Ma.|||Intrudes Halls Creek Group.|Sill-like bodies.|
27939|Woodward Dolerite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 1m_geologyl12_lithology_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyl12_lut.csv.|1847-1808 Ma (inferred)||||Fine- to coarse-grained metadolerite, and minor amphibolite|
27939|Woodward Dolerite|71397|4|Described|p1,3-5,18,25-28,30,46,48|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen. Emplaced and intruded into Sophie Downs Suite and Halls Creek Group at onset of c. 1832-1808 Halls Creek Orogeny. Not directly dated; overprinted by D2/M2 Halls Creek Orogeny places a minimum age at 1808 Ma. Sill-like intrusive bodies up to 200 m thick. Metamorphosed in the upper greenschist to epidote-amphibolite facies (Blake et al., 1999b). Geochemical analysis indicate a subalkaline basalt or basaltic andesite affinity. See p25-27 for detailed major and trace-element geochemical analysis. Sm-Nd whole-rock isotope analysis showed ENd values between -0.856 and +3.05, with a 1835 Ma TDM2 model age. Geochemically similar to Ding Dong Downs Volcanics, and the mafic rocks of Brim Rockhole and Biscay formations. Nd isotopic values indicate a primitive source; trace-element analysis show evidence of crustal contamination. Represents final episode of lithospheric mantle tapping prior to onset of Halls Creek Orogeny.|c. 1835 Ma|||Intrudes into Halls Creek Group and Sophie Downs Suite.||
27939|Woodward Dolerite|71873|5|Briefly described|p426-427|Orosirian|Orosirian|Geological province: Lamboo Province. Intrudes into Sophie Downs Suite and Halls Creek Group during c. 1832-1808 Ma Halls Creek Orogeny.|c. 1835 Ma|||||
27939|Woodward Dolerite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Halls Creek Orogen.|||||Fine- to coarse-grained metadolerite, and minor amphibolite.|
27939|Woodward Dolerite|72437|5|Briefly described|p8, p56, p58|||Analysed 12 times for whole-rock analysis and REE.||||Intrudes the Biscay Formation and the Olympio Formation.|Dolerite and metadolerite.|
34583|Woodynook Sandstone|12758|5|Briefly described|p13, p3 Fig. 3|Early Permian|Early Permian|Of the Sue Group.  Predominantly poorly sorted fluvial sandstone.  Conformably overlain by Rosabrook Coal Measures.  Max. thickness: 121m; only 71m in type section.  Geological Province: Southern Perth Basin.||||||
34583|Woodynook Sandstone|14227|5|Briefly described|Enclos. 2|Sakmarian|Asselian|Basal unit of the Sue Group. Underlies Rosabrook Coal Measures; overlies Mosswood Formation. Geol. Prov: Bunbury Trough, southern Perth Basin.||||||07-FEB-11
34583|Woodynook Sandstone|22818|5|Briefly described|map|Early Permian|Early Permian|Of the Sue Group.||||||12-AUG-08
34583|Woodynook Sandstone|22819|5|Briefly described|map|Early Permian|Early Permian|Of the Sue Group.||||||12-AUG-08
34583|Woodynook Sandstone|22820|2|Defined|p8-9 Tbs.1& 2, p15-16|Early Permian|Early Permian|Of Sue Group. No coal seams. Thickness: up to 70m. Geol.prov: south Perth Basin. Predominantly sandstone with interbedded conglom+subordinate argillaceous units; transitional between Mosswood Fm below and Rosabrook CM above. detailed lith. included.||||||29-APR-09
34583|Woodynook Sandstone|24443|5|Briefly described|Fig.31|Early Permian|Early Permian|Basal unit of Sue Group. Conformably overlies Mosswood Formation. Conformably overlain by Rosabrook Coal Measures. Geological Province: Perth Basin.||||||
34583|Woodynook Sandstone|50107|5|Briefly described|Map legend|Permian|Permian|Of the Sue Group. Geological Province: Southern Perth Basin.||||||13-DEC-07
34583|Woodynook Sandstone|60386|5|Briefly described|p296, 309|Artinskian|Artinskian|Southern Perth Basin. Non-marine.||||||
34583|Woodynook Sandstone|64630|5|Briefly described|p31 Fig.2|Sakmarian|Sakmarian|Province: Southern Perth Basin. Overlies the Mosswood Formation, underlies the Rosabrook Coal Measures. Palynology age: P. pseudoreticulata. Base correlates with the base of the Westralia Sandstone.||||||
34583|Woodynook Sandstone|67925|4|Described|Ch2 p10 fig 4, Ch2 p11-p13|Sakmarian|Sakmarian|A type section in the Sue 1 drillhole is 121m thick. Palynology discussed. See also Ch2 p20, Ch2 p30, Ch3 p8, Ch4 p8 fig 2.||Sue Group||Overlies the Mosswood Formation. Conformably overlain by the Rosabrook Coal Measures.|Poorly sorted fluvial sandstone.|
34583|Woodynook Sandstone|69029|6|Mentioned|p332|Cisuralian|Cisuralian|Of Perth Basin.||||Overlain by High Cliff Sandstone. Underlain by Holmwood Shale.||
34583|Woodynook Sandstone|69081|5|Briefly described|p737 Fig.1|Cisuralian||Presented as Woodynook Sst in figure. Geol. Prov: Perth Basin.||Sue Group||Is overlain by Rosabrook Coal Measures; overlies Mosswood Formation.||23-JUL-15
34583|Woodynook Sandstone|69182|6|Mentioned|Ch2 p9, Ch2 p45, Ch2 p47|Early Permian|Early Permian|Perth Basin. [May be incorrectly assigned by the author to the Stockton Group as oppossed to the Sue Group.] See also Ch2 p55, Ch2 p57, Ch2 p60, Ch2 p64-p66, Ch2 p80, Ch2 p84, Ch2 p91, Ch2 p92, Ch2 p94-p96, Ch2 p98, Ch2 p100, Ch2 p102, Ch2 p104, Ch2 p106, Ch2 p108, Ch2 p110.||Stockton Group||Overlies the Mosswood Formation. Overlain by the Rosabrook Coal Measures.||
34583|Woodynook Sandstone|69297|6|Mentioned|p175, p187,  p189|Artinskian|Sakmarian|Vlaming Sub-basin, South Perth Basin. ||Sue Group||Overlies the Mosswood Formation. Overlain by the Rosabrook Coal Measures.||
34583|Woodynook Sandstone|70097|5|Briefly described|p2, p19 Fig.3|Sakmarian|Sakmarian|Southern Perth Basin. Bunbury Trough.||Sue Group||Overlies Mosswood Formation (Stockton Group). Is overlain by Rosabrook Coal Measures.|Pro-glacial marine basin fill. Includes sandstone.|13-SEP-17
34583|Woodynook Sandstone|70099|5|Briefly described|Fig.4|Sakmarian|Sakmarian|||Sue Group.||Overlies Mosswood Formation (Stockton Group). Is overlain by Rosabrook Coal Measures.||
34583|Woodynook Sandstone|70128|5|Briefly described|p449|Permian|Permian|Southern Perth Basin.||Sue Group.||Conformably overlies Mosswood Formation. Is overlain conformably by Rosabrook Coal Measures.||
34583|Woodynook Sandstone|70774|5|Briefly described|p5 fig 3|Sakmarian|Sakmarian|Southern Perth Basin.||||Overlies the Mosswood Formation. Overlain by the Rosabrook Coal Measures.||
34583|Woodynook Sandstone|71146|5|Briefly described|p6|Artinskian|Sakmarian|Perth Basin.||||Overlies the Mosswood Formation. Overlain by the Rosabrook Coal Measures.|Sandstone.|
34583|Woodynook Sandstone|71377|5|Briefly described|p7|Permian|Permian|Perth Basin.||Stockton Group||||
34583|Woodynook Sandstone|71958|5|Briefly described|p34|Sakmarian|Sakmarian|Vlaming Sub-basin.||Sue Group||Overlies the Mosswood Formation. Overlain by the Rosabrook Coal Measures.||
34583|Woodynook Sandstone|72258|5|Briefly described|p129|Cisuralian|Cisuralian|Of Perth Basin.||||Overlain by Rosabrook Coal Measures. Underlain by Mosswood Formation.||
35375|Woolgangie Supersuite|23904|5|Briefly described|p27, p64|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
35375|Woolgangie Supersuite|60667|5|Briefly described|p1126 Fig. 2, p1138|Archean|Archean|Age: 2646+/-6Ma (Hill et al 1992).  Includes the Boorabin batholith.  See also p1136 Fig. 6.||||||07-NOV-08
35375|Woolgangie Supersuite|65834|6|Mentioned|p17||||||||Granitoids.|
74952|Woolgra Andesite Member|64891|6|Mentioned|p48-9 Tb. 1|||||||||07-FEB-11
74952|Woolgra Andesite Member|67129|5|Briefly described|p18 Fig.19|Archean|Archean|Murchison Domain, Youanmi Terrane.|c.2761 Ma.|Greensleeves Formation.||||07-SEP-17
74952|Woolgra Andesite Member|68110|5|Briefly described|p674 Fig. 2|Neoarchean|Neoarchean|Murchison Domain. Age constrained by that of the parent Greensleeves Formation.|c. 2761-2734 Ma|Of the Greensleeves Formation.|||Andesitic volcanic rocks.|
74952|Woolgra Andesite Member|68561|5|Briefly described|GEOCHRON files|Neoarchean|Neoarchean|Possible lateral equivalent of this unit dated: 2761 +/- 6 Ma. From geochron file 185957.1.pdf.|2755+/- 5 Ma (GSWA 178105, Wingate et al., 2008).|Greensleeves Formation||||
74952|Woolgra Andesite Member|68698|5|Briefly described|p7, p11|||Igneous crystallisation age.|2755 +/- 5 Ma (Wingate et al., 2008).|Greensleeves Formation.||Overlies Meekatharra Formation.||
74952|Woolgra Andesite Member|69583|5|Briefly described|p49, Plate 2|Neoarchean|Neoarchean|Murchison Domain.||Greensleeves Formation.|||Metamorphosed volcaniclastic andesite.|
74952|Woolgra Andesite Member|69584|5|Briefly described|p5 Fig.2|Neoarchean|Neoarchean|||Greensleeves Formation||||
74952|Woolgra Andesite Member|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Greensleeves Formation.||||
74952|Woolgra Andesite Member|70796|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Younami Terrane. See also 185957.1.pdf, 185959.1.pdf|2755 +/ 5 Ma (isotopic)|Greensleeves Formation||||
74952|Woolgra Andesite Member|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv.|2755+\-5 Ma|Unit of Greensleeves Formation.|||Volcaniclastic andesite; metamorphosed|
74952|Woolgra Andesite Member|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|c.2755 Ma.|Greensleeves Formation.|||Metamorphosed volcaniclastic andesite.|
74952|Woolgra Andesite Member|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Youanmi Terrane. |2755+/-5 Ma.|Greensleeves Formation|||Volcaniclastic andesite; metamorphosed.|
74952|Woolgra Andesite Member|72389|5|Briefly described|Map Legend|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Gabanintha 1:100k map sheet 2644.|~2755 Ma.|Greensleeves Formation|||Volcaniclastic andesite; metamorphosed.|28-AUG-20
70705|Woolnough Member|62453|3|Fully described|p13, 19, 24|Cryogenian|Cryogenian|Stromatolitic carbonate, dolomite, siltstone, limestone. Previously Woolnough Formation. Of Browne Formation. Correlated with Skates Hills Formation and Loves Creek Member.||||||16-JAN-07
70705|Woolnough Member|63022|5|Briefly described|p1016 Fig. 2|Neoproterozoic|Neoproterozoic|Of the Browne Formation. Geological Province: Officer Basin. Red-grey stromatolitic dolostone, mudstone.||||||10-AUG-07
70705|Woolnough Member|65363|5|Briefly described|p6 Fig.5, pp10-11, p37. |Neoproterozoic|Neoproterozoic|Formerly 'Woolnough beds' (Jackson and van de Graaff 1981). Presence of Acaciella australica Stromatolite Assemblage enables correlation with Skates Hill Formation, Loves Creek Member of the Bitter Springs Formation, Yackah beds, and Coominaree Dolomite.||Unit in Browne Formation.|||Red-grey stromatolitic dolostone, argillaceous dolostone, dolomitic mudstone, and minor dolomitic sandstone.|
70705|Woolnough Member|65364|5|Briefly described|p81|||Officer Basin.||Of Browne Formation.|||Red-grey stromatolitic dolostone, mudstone.|16-MAR-12
70705|Woolnough Member|65365|5|Briefly described|p6, p8 Fig 3|||Member of the Browne Formation.||||||19-MAR-12
70705|Woolnough Member|65366|5|Briefly described|p19, 21, 24|Cryogenian|Cryogenian|Pinkish dolomite.Member of the Browne Formation. Includes the Acaciella australica Stromatolite Assemblage||||||19-MAR-12
70705|Woolnough Member|65371|5|Briefly described|p54 Fig. 1|||Of Browne Formation. Stromatolitic dolostone and mudstones; shallow marine depositional environment||||||
70705|Woolnough Member|67454|5|Briefly described|p563 Fig.2, p564.|Neoproterozoic|Neoproterozoic|Officer Basin.||Unit in Browne Formation.|||Stromatolitic dolostone and mudstone.|
70706|Wooltanna Volcanics|62453|6|Mentioned|p13, 24|||Correlated with the Cadlareena Volcanics||||||
81974|Wooly Formation|72712|5|Briefly described|p33-34, p42, p45, p9.|Orosirian|Orosirian|Revision of Wooly Dolomite, due to lithological variability. Significantly more extensive than original Wooly Dolomite. Includes rocks previously mapped as Mount McGrath Formation. Excluded from both Shingle Creek and Wyloo Groups. See also p48, p53.|< 2031 +/- 6 Ma.|||Unconformably overlies Cheela Springs Basalt and unconformably underlies Mount McGrath Formation.|A succession of locally stromatolitic dolomite that overlies a basal pebbly arenite. Contains a substantial proportion of conglomerate, sandstone, siltstone and mudstone.|14-JAN-21
29565|Woongarra Rhyolite|22622|6|Mentioned|p223|||||||||
29565|Woongarra Rhyolite|22689|6|Mentioned|Fig. 1 p138|||Of Hamersley Group.||||||
29565|Woongarra Rhyolite|23046|6|Mentioned|171|||||||||
29565|Woongarra Rhyolite|23047|6|Mentioned|35|Palaeoproterozoic|Palaeoproterozoic|Of the Hamersley Group. Hamersley Province.  Age 2449 +/-3 Ma. Overlying unit Boolgeeda Iron Formation||||||10-FEB-09
29565|Woongarra Rhyolite|23280|5|Briefly described|p1087,Table1p1085||Siderian|Max Age: 2449 (+/-) 3 Ma.||||||
29565|Woongarra Rhyolite|23570|5|Briefly described|p14|Archean|Archean|Of Hamersley Group. Previously named Woongarra Volcanics. Geological Province: Pilbara Craton||||||07-NOV-08
29565|Woongarra Rhyolite|23575|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Hamersley Group. Overlying unit Boolgeeda Iron Formation. Underlying unit Weeli Wolli Formation.||||||
29565|Woongarra Rhyolite|23890|5|Briefly described|p5 Fig.2|||Of Hamersley Group. Age: 2449+/-3Ma (U-Pb SHRIMP).  Geological Province: Hamersley Basin.||||||
29565|Woongarra Rhyolite|24041|6|Mentioned|p492|||||||||
29565|Woongarra Rhyolite|24115|5|Briefly described|p27|Paleoproterozoic|Paleoproterozoic|Age: 2.45 Ga.||||||07-NOV-08
29565|Woongarra Rhyolite|24185|5|Briefly described|p750|Siderian|Archean|Age: ca. 2450 Ma. Parent: Hamersley Group. Geological Province: Pilbara Craton.||||||07-NOV-08
29565|Woongarra Rhyolite|24544|4|Described|p47 Fig.35, p57 Fig.43|Siderian|Siderian|Age: 2449+/-3 Ma. Of Hamersley Group. Overlies Weeli Wooli Formation. Overlain conformably by Boolgeeda Iron Formation. Contains several flows. Geological Province: Hamersley Basin.||||||01-FEB-05
29565|Woongarra Rhyolite|24607|5|Briefly described|p969 Fig. 2|||Of the Hamersley Group.||||||
29565|Woongarra Rhyolite|42986|4|Described|p391|||Variation on Woongarra Volcanics?||||||
29565|Woongarra Rhyolite|43262|5|Briefly described|Map Legend||Proterozoic|of Hamersley Group.||||||
29565|Woongarra Rhyolite|43290|4|Described|p7||Proterozoic|Of Hamersley Group. U-Pb age of 2470+/-30 Ma,1981. Formerly Woongarra Volcanics.||||||15-DEC-08
29565|Woongarra Rhyolite|60706|5|Briefly described|p623, p630, p643 App.1|Paleoproterozoic|Paleoproterozoic|Supersedes both Wongarra Dacite and Woongarra Volcanics. Of the Hamersley Group. Underlies the Bolgeeda Iron Formation; overlies the Weeli Wolli Formation. Age: 2449+/-3 Ma (SHRIMP), 2445+/-5 MA, 2451+/-5 Ma. Max. thickness: >400m.||||||07-NOV-08
29565|Woongarra Rhyolite|62129|3|Fully described|p10|Archaean|Archaean|Of Hamersley Group. Conformably overlies Weeli Wolli Formation. Age: 2470+/-30 and 2439+/-10Ma (U-Pb zircon). Thickness: 800m. Geological Province: Hamersley Basin.||||||19-SEP-13
29565|Woongarra Rhyolite|62130|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Hamersley Group. Geological Province: Hamersley Basin, Pilbara Craton. Metamorphosed rhyolite, rhyodacite, rhyolitic breccia, and banded iron-formation.||||||23-MAR-09
29565|Woongarra Rhyolite|63372|4|Described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Hamersley Group. Geological Province: Hamersley Basin. Age: 2449Ma. Rhyolite, rhyodacite, rhyolitic volcanoclastic breccia, and banded iron formation. Underlies: Boolgeeda Iron Formation. Overlies: Weeli Wolli Formation.||||||07-NOV-08
29565|Woongarra Rhyolite|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Of Upper Hamersley Group. Rhyolite, rhyodacite, rhyolitic breccia, and banded iron-formation; metamorphosed.||||||15-DEC-08
29565|Woongarra Rhyolite|64725|5|Briefly described|p58.|||A large concordant felsic sill.|c.2440 Ma.|Unit in Hamersley Group.||Overlies Weeli Wolli Formation. Is overlain by Boolgeeda Iron-formation.||
29565|Woongarra Rhyolite|64830|4|Described|p1107-8|Archaean|Archaean|Of Hamersley Gp. Below Boolgeeda Iron Fm. Age: 2439+/-10Ma. Max.thick:~300m.Geol.prov:Hamersley Basin (Ophthalmia Range).Massive lava+ash flow tuffs, predom'ly K-feldspar-phyric rhyodacite+rhyolite. Hosts Hickman Crater at contact with Woongarra Rhyolite.||||||23-MAR-09
29565|Woongarra Rhyolite|66574|5|Briefly described|p912, p914 Fig.3||Siderian|Upper Hamersley Group. Underlies Boolgeeda Iron Formation. Backarc felsic volcanic rocks and intrusions. c.2450 Ma. Called Woongarra Volcanics in Fig.9.||||||
29565|Woongarra Rhyolite|66887|5|Briefly described|p21 Fig.11|||Pilbara Craton. Woongarra Rhyolite/Weeli Wolli Formation shown together with single age in Fig.11.|~2500 Ma estimated from Fig.11.|||||
29565|Woongarra Rhyolite|67056|5|Briefly described|p419 Fig.2, p423. |||Occurs throughout the Hamersley Province. Originally considered extrusive, now regarded as intrusive. Over 15,400 cubic kilometres of felsic lava. ||Unit in Hamersley Group.||Intrudes Hamersley Group.||
29565|Woongarra Rhyolite|67130|5|Briefly described|p3 fig 2, p24 fig 17,|Siderian|Siderian|Also referred to as Woongarra Volcanics - an outdated name (p8 fig 5). See also p38, p39 fig 36, p40 fig 37. |c. 2445 Ma|Hamersley Group||Overlies Brockman Iron Formation, Yandicoogina Shale Member, Weeli Wolli Formation, overlain by Boolgeeda Iron Formation|Rhyolitic lava, rhyolitic breccia|
29565|Woongarra Rhyolite|67201|5|Briefly described|p34, p53 Fig.40, p56|||Interpreted as intrusive, sill-like unit. Common source for lower Turee Creek Group.|c. 2450 Ma zircon SHRIMP U-Pb Trendall et al. 2004|Hamersley Group||Overlies Weeli Wolli Formation. Is overlain by Boolgeeda Iron Formation.||25-NOV-16
29565|Woongarra Rhyolite|67721|5|Briefly described|p38 Fig.9|Siderian|Siderian|Between 300-700 m thick.|c. 2449 Ma|Of the Hamersley Group.||||
29565|Woongarra Rhyolite|68035|5|Briefly described|p292, Fig 6|Paleoproterozoic|Paleoproterozoic|Hamersley Basin. Interpreted by Trendall (1995) as an intrusive, sill-like unit, although it also has obvious extrusive portions.|2450+/-3 Ma|Of Hamersley Group.||Overlies Weeli Wolli Formation. Overlain by Boolgeeda Iron Formation.|Rhyolite.|
29565|Woongarra Rhyolite|68280|5|Briefly described|p5, p41, p47, p54, p62|Paleoproterozoic|Paleoproterozoic||2450 Ma|Hamersley Group||Overlain by Boolgeeda Iron Formation, overlies Weeli Wolli Formation|Rhyolite, rhyolite breccia with dark-weathering fiamme and rounded to angular clasts of porphyritic rhyolite in a fine grained matrix.|
29565|Woongarra Rhyolite|69003|6|Mentioned|p7|||Associated with the Ophthalmian Orogeny.||||||
29565|Woongarra Rhyolite|69028|5|Briefly described|Map Legend|Siderian|Siderian|Hamersley Basin.||Of the Hamersley Group.|||Rhyolite, rhyodacite, rhyolitic breccia, and banded iron-formation; metamorphosed.|07-MAY-14
29565|Woongarra Rhyolite|69166|5|Briefly described|500k_geologyp08_lut.csv|Neoarchean|Neoarchean|||Hamersley Group|||Rhyolite, rhyodacite, rhyolitic breccia, and banded iron-formation; metamorphosed.|
29565|Woongarra Rhyolite|69185|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological Province: Pilbara Craton. Of Northwest, Northeast, and South Pilbara Sub-basins, Hamersley Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.||Unit of Hamersley Group.|||Rhyolite, rhyodacite, rhyolitic breccia, and banded iron-formation; metamorphosed|
29565|Woongarra Rhyolite|69538|6|Mentioned|p517 Fig.3, p530, p532 Tb.3, p579|Paleoproterozoic|Paleoproterozoic|Appears as Woongarra Formation on p530 and 532.||Unit in Hamersley Group.||||
29565|Woongarra Rhyolite|69565|6|Mentioned|p132, p133 Fig.1|||Barley et al. (1997). First presented as Wongara rhyolite.|2449 +/- 3 Ma.|Hamersley Group.||Overlies Weeli Wolli Formation. Is overlain by Boolgeeda Iron Formation.||
29565|Woongarra Rhyolite|69590|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|Of Hamersley Basin. Events: Paterson Orogeny; Miles Orogeny.||Unit of Hamersley Group.|||Rhyolite, rhyodacite, rhyolitic breccia, and banded iron-formation; metamorphosed|
29565|Woongarra Rhyolite|69745|6|Mentioned|p276|||Mount Wall area, Hamersley Province. See also references to Woongarra Formation (p272-276, 281, 283-284, 287).||||Is faulted against Joffre Member.||
29565|Woongarra Rhyolite|69754|6|Mentioned|p315, p331|Siderian|Siderian|Pilbara Craton.|c. 2449+/- 3 Ma|||Conformably overlain by the Boolgeeda Iron Formation.||
29565|Woongarra Rhyolite|70086|5|Briefly described|p195-196|Siderian|Siderian|Geological province: Pilbara Craton. Of the Hamersley Basin.|2449+\-3 Ma|Unit of Hamersley Group.||Overlain by Boolgeeda Iron Formation. Underlain by Weeli Wolli Formation.||
29565|Woongarra Rhyolite|70795|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|West Australian Craton, Hamersley Basin|2449-2445 Ma||||Rhyolite, rhyodacite, rhyolitic breccia and banded iron formation; metamorphosed.|
29565|Woongarra Rhyolite|71112|5|Briefly described|p84-85|||Geological province: Pilbara Craton. Back-arc bimodal magmatism along an active margin on the SW margin of the Hamersley Province. Interpreted as a condensed section with the overlying Boolgeeda Iron Formation (starved basin). Zircon age dating from Barley et al., 1997.|2455-2443 Ma|||Overlain by Boolgeeda Iron Formation.|Submarine-erupted pillow basalts, basaltic hyaloclastites and subvolcanic dolerite sills, overlain by submarine-emplaced rhyolite domes, interlayered BIFs, and upper mixed volcaniclastic and siliciclastic rocks.|
29565|Woongarra Rhyolite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||rhyolite, rhyodacite, volcanic breccia, banded iron formation|
29565|Woongarra Rhyolite|71550|5|Briefly described|p35,37,44-45|Siderian|Siderian|Geological province: Of Hamersley Basin. Contains U-Pb zircon dates at 2450+\-3 Ma (Barley et al., 1997; Trendall et al., 2004).|c. 2.45 Ga|||Overlain by Boolgeeda Iron Formation,||03-SEP-19
29565|Woongarra Rhyolite|71808|4|Described|viii, p34, p40-p42, p46-p47|||Hamersley Province. Up to 400m thick. Can be subdivided into three informal unnamed units: a lower rhyolite; Median raft complex and an upper rhyolite. Rhyolites are interpreted as intrusive based on peperites and variation in the raft complex. Apparent on airphotos as a poorly exposed, orange toned unit between more resistive BIF's of the Weeli Wolli and Boolgeeda Iron formations. See also  p73, p85, p103, p117, p149, p156, p210.||Hamersley Group||Overlies the Weeli Wolli Formation. Overlain by the Boolgeeda Iron Formation.|Two rhyolites seperated by an impersistent unit of BIF, dolerite and shale.|
29565|Woongarra Rhyolite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Hamersley Basin.|Max age 2449+/-3 Ma, min 2445+/-5 Ma|Hamersley Group, upper|||Rhyolite, rhyodacite, rhyolitic breccia, and banded iron-formation; metamorphosed.|
29565|Woongarra Rhyolite|72493|5|Briefly described|p30|||Hamersley Basin.||Hamersley Group.||Overlies Weeli Wolli Formation. Is overlain by Boolgeeda Iron Formation.|Mostly rhyolite; minor BIF.|
29565|Woongarra Rhyolite|72570|6|Mentioned|p2|Siderian|Siderian||2449 +/- 3 Ma (Barley et al, 1997)|Hamersley Group||Conformably overlies the Boolgeeda Iron Formation.|Rhyolite|
29565|Woongarra Rhyolite|72705|5|Briefly described|p14||||c.2450 Ma.||||Felsic volcanics.|
29565|Woongarra Rhyolite|72712|4|Described|p11-13, p14, p40, p42-47, p57, p9|Siderian|Siderian|See also p11 Fig.8, p13, p43, p55. Previously interpreted as an intrusive unit. Old Rb-Sr dating has been superseded. Could be as young as c. 2419 Ma based on the single-zircon TIMS analyses of Pidgeon and Horwitz (1991), but most reliable igneous crystallisation age is 2444+/-3 Ma (GSWA 195892, Wingate et al, 2018).This formation is well exposed in a creek section along the Beasley River at Woongarra Pool.|2444+/-3 Ma SHRIMP U-Pb?|Hamersley Group||Shown as overlying Weeli Wolli Formation, disconformably underlying Boolgeeda Iron Formation.|Rhyolite.|
29565|Woongarra Rhyolite|73022|6|Mentioned|p2 Fig.1|||||Hamersley Group||Overlies the Weeli Wolli Formation, underlies the Boolgeeda Iron Formation.||
29565|Woongarra Rhyolite|73102|6|Mentioned|p4|||Intruded by a north-northeasterly trending dolerite dyke.|c. 2450 Ma|Hamersley Group||||
29565|Woongarra Rhyolite|73538|5|Briefly described|p1-7|Siderian|Siderian|[Also misspelt as Woogarra Rhyolite on p2]. A zircon U-Pb age of 2455 +/- 3 Ma was reported by Trendall et al. (2004).|2455 +/- 3 Ma|Hamersley Group||Underlain by Weeli Wolli Formation. Overlain by Boolgeeda Iron Formation.|Includes felsic volcanics and minor mafic volcanics and iron formation.|
25651|Wooramel Group|12731|6|Mentioned|p591 Fig.3.|||||||Overlies Callytharra Formation. Is overlain by Kennedy and Byro Groups.||
25651|Wooramel Group|12733|5|Briefly described|p554 Fig.2, p565.|Early Permian|Early Permian|Sakmarian-Artinskian. Gaseous source in Merlinleigh Sub-basin, decreasing from north to south. Marine shales expected to act as source and seal for Moogooloo Sandstone. Excellent in organic richness but only fair to very good in generating potential.||||Overlies Callytharra Formation. Is overlain by Byro Group.|Predominantly clastic shallow marine deposits.|
25651|Wooramel Group|13615|6|Mentioned|p58|||||||||
25651|Wooramel Group|14228|5|Briefly described|p1, p5 fig 2, p8, p10, p14-17, p20-21|Artinskian|Artinskian|Petroleum source beds. Northern Merlinleigh Sub-basin. The group is thickest in the northwestern part of the Sub-basin.|||Includes Cordalia Formation, Moogooloo Sandstone, Billidee Formation.|Overlies Callytharra Formation. Overlain (conformably) by Byro Group.|Predominantly fluvial- to marine-deltaic sandstone facies; minor shale and coal.|
25651|Wooramel Group|22814|5|Briefly described|fig2|Early Permian|Early Permian|||||||
25651|Wooramel Group|22817|5|Briefly described|p1|Early Permian|Early Permian|Carnarvon Basin||||||
25651|Wooramel Group|23174|5|Briefly described|Fig5p8|Permian|Permian|||||||
25651|Wooramel Group|23310|5|Briefly described|Map legend|Artinskian|Artinskian|||||||
25651|Wooramel Group|23311|5|Briefly described|map legend|Artinskian|Artinskian|||||||
25651|Wooramel Group|23312|5|Briefly described|map legend|Artinskian|Artinskian|||||||
25651|Wooramel Group|23403|4|Described|p7|Late Permian|Middle Devonian|||||||24-NOV-09
25651|Wooramel Group|23569|4|Described|p4 Tb. 1|Early Permian|Early Permian|Includes the Keogh Formation and Moogooloo Sandstone.||||||
25651|Wooramel Group|23574|5|Briefly described|Map Legend|Early Permian|Early Permian|Overlying unit Byro Group. Underlying unit Lyons Group.||||||
25651|Wooramel Group|23576|5|Briefly described|Map Legend|Early Permian|Early Permian|Overlying unit Byro Group. Underlying unit Lyons Group.||||||
25651|Wooramel Group|23577|5|Briefly described|Map Legend|Early Permian|Early Permian|Overlying unit Byro Group. Underlying unit Lyons Group.||||||
25651|Wooramel Group|23620|5|Briefly described|p4 Fig. 4|Permian|Permian|||||||
25651|Wooramel Group|23726|5|Briefly described|p37|Late Permian|Early Permian|Overlying unit Byro Group. Geological Province: Byro Sub-basin.||||||
25651|Wooramel Group|23815|4|Described|p281|||Formerly known as the "Wooramel Sandstone". Geological Province: Carnarvon Basin. Overlying unit: Byro Group (conformable). Underlying unit: Callytharra Formation (disconformable).||||||
25651|Wooramel Group|23976|5|Briefly described|Map Legend|Phanerozoic|Phanerozoic|||||||
25651|Wooramel Group|23977|5|Briefly described|Map Legend|Phanerozoic|Phanerozoic|||||||
25651|Wooramel Group|23978|5|Briefly described|Map Legend|Phanerozoic|Phanerozoic|||||||
25651|Wooramel Group|24044|5|Briefly described|p541 Fig.2|Early Permian|Early Permian|||||||
25651|Wooramel Group|24059|5|Briefly described|p137|Permian|Permian|Geological Province: Carnarvon Basin.  Maximum thickness: 500m.||||||
25651|Wooramel Group|24114|5|Briefly described|p8|||Geological Province: Carnarvon Basin.||||||
25651|Wooramel Group|24390|5|Briefly described|p19 Fig. 10|Permian|Permian|Geological Province: Southern Carnarvon Basin.||||||
25651|Wooramel Group|24410|5|Briefly described|p137 Fig. 80|Permian|Permian|Includes Moogooloo Sandstone and Billidee and Keogh Formations. Sandy, silty sequenceof sandstone, siltstone and shale. Geological Province: Carnarvon Basin.||||||24-NOV-09
25651|Wooramel Group|30545|6|Mentioned|p22|||Correlation. See also P23||||||
25651|Wooramel Group|31561|5|Briefly described|p34|||See also p32. Artinskian - Tatarian ? Hydrocarbon potential.||||||11-FEB-19
25651|Wooramel Group|32113|4|Described|p47|||re environment of deposition||||||
25651|Wooramel Group|32648|6|Mentioned|p32|||L.Permian||||||
25651|Wooramel Group|32945|6|Mentioned|p73|||See also P88. Sakmarian||||||
25651|Wooramel Group|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
25651|Wooramel Group|33386|6|Mentioned|Fig.7|||||||||
25651|Wooramel Group|33450|6|Mentioned|Fig.5|||||||||
25651|Wooramel Group|33453|4|Described|p70|||Artinskian.||||||
25651|Wooramel Group|33594|6|Mentioned|p37|||||||||
25651|Wooramel Group|33701|6|Mentioned|Fig.1|||Artinskian.||||||
25651|Wooramel Group|33711|6|Mentioned|p384|||Table 4.||||||
25651|Wooramel Group|34008|6|Mentioned|p71|||L.Permian||||||
25651|Wooramel Group|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
25651|Wooramel Group|34532|6|Mentioned|p225|||||||||
25651|Wooramel Group|34846|6|Mentioned|Fig.3|||||||||
25651|Wooramel Group|35144|6|Mentioned|Fig.5|||||||||
25651|Wooramel Group|35282|6|Mentioned|Fig.2|||||||||
25651|Wooramel Group|36020|6|Mentioned|p393|||||||||
25651|Wooramel Group|36257|6|Mentioned|Table 2.1|||||||||
25651|Wooramel Group|36890|3|Fully described|p281|||Formerly Wooramel Sandstone||||||
25651|Wooramel Group|36902|6|Mentioned|p22|||||||||
25651|Wooramel Group|37294|6|Mentioned|p100|||||||||
25651|Wooramel Group|37295|4|Described|p53|||See also p51.||||||11-FEB-19
25651|Wooramel Group|37304|6|Mentioned|p55|||||||||
25651|Wooramel Group|37920|6|Mentioned|p457|||||||||
25651|Wooramel Group|38482|6|Mentioned|p22|||||||||
25651|Wooramel Group|38493|4|Described|p34|||||||||
25651|Wooramel Group|38494|4|Described|p30|||See also p19.||||||11-FEB-19
25651|Wooramel Group|38998|6|Mentioned|p34|||||||||
25651|Wooramel Group|39316|6|Mentioned|Fig.2|||||||||
25651|Wooramel Group|39370|4|Described|p35|||||||||
25651|Wooramel Group|39427|4|Described|Table 1|||||||||
25651|Wooramel Group|40336|5|Briefly described|p18|||||||||
25651|Wooramel Group|40339|6|Mentioned|Map legend|Artinskian|Artinskian|||||||
25651|Wooramel Group|40340|6|Mentioned|p20|||||||||
25651|Wooramel Group|40617|6|Mentioned|Fig.1|||||||||
25651|Wooramel Group|40794|6|Mentioned|p91|||||||||
25651|Wooramel Group|40992|6|Mentioned|Fig.8|||||||||
25651|Wooramel Group|41172|6|Mentioned|p121|||||||||
25651|Wooramel Group|41271|3|Fully described|p80|||Formerly "Wooramel Sandstone"||||||
25651|Wooramel Group|41436|6|Mentioned|p42|||||||||
25651|Wooramel Group|41438|4|Described|p104|||||||||
25651|Wooramel Group|41443|6|Mentioned|p163|||||||||
25651|Wooramel Group|41444|6|Mentioned|Fig.4|||||||||
25651|Wooramel Group|41446|6|Mentioned|Fig.17|||||||||
25651|Wooramel Group|41689|6|Mentioned|Table 1|||||||||
25651|Wooramel Group|42116|5|Briefly described|p27|||||||||
25651|Wooramel Group|42392|5|Briefly described|p115|||||||||
25651|Wooramel Group|42462|4|Described|p55|||||||||
25651|Wooramel Group|43015|5|Briefly described|Table 1,p319|||||||||
25651|Wooramel Group|43018|5|Briefly described|Table 1,p386|||||||||
25651|Wooramel Group|43255|5|Briefly described|map legend||Artinskian|||||||
25651|Wooramel Group|43256|5|Briefly described|5, 20||Permian|||||||
25651|Wooramel Group|43835|5|Briefly described|Map Legend||Artinskian|||||||
25651|Wooramel Group|44040|14|Not recorded|p43|||||||||
25651|Wooramel Group|44219|14|Not recorded|Not recorded||Artinskian|||||||
25651|Wooramel Group|44344|14|Not recorded|p.10-11,opp.4, map||Artinskian|Includes Artinskian Moogooloo Sandstone & Billidee Formation. (G50-1).||||||
25651|Wooramel Group|44345|14|Not recorded|map legend||Artinskian|Artinskian.||||||
25651|Wooramel Group|44532|4|Described|p.6, map|||(G50-5).||||||
25651|Wooramel Group|44533|5|Briefly described|map legend||Artinskian|Artinskian.||||||
25651|Wooramel Group|44994|6|Mentioned|Fig.7|||Correlation.Perm.||||||
25651|Wooramel Group|45001|14|Not recorded|p7, p146|Artinskian|Artinskian|Of Carnarvon Basin.||||||25-NOV-16
25651|Wooramel Group|45015|5|Briefly described|map legend|Artinskian|Artinskian|Includes: Cordalia Greywacke, Moogooloo and Nunnery Sandstones, Monument Formation. Jimba Jimba Calcarenite, Curbur, Congo, One Gum, Billidee and Keogh Formations. Geological Province: Carnarvon Basin.||||||29-JAN-08
25651|Wooramel Group|45016|2|Defined|p74-77||Artinskian|Tb, p.12,57,64,68,79,82,91,102-3,105,109,118,121,125,126,132,146,150. (F49-12,F50-9,13,G50-1,2,5,6,9,10).||||||
25651|Wooramel Group|46849|6|Mentioned|Fig. 6|||||||||
25651|Wooramel Group|47041|6|Mentioned|Fig.2|||||||||
25651|Wooramel Group|48610|4|Described|p4|||||||||
25651|Wooramel Group|48628|14|Not recorded|Fig.5|||(F50-5/Onslow).||||||
25651|Wooramel Group|48885|14|Not recorded|p.9-11,13,17||Early Permian|Lower Permian (Sakmarian-Artinskian).||||||
25651|Wooramel Group|49644|5|Briefly described|Table|||||||||
25651|Wooramel Group|50085|5|Briefly described|p19 Fig. 10|Permian|Permian|Geological Province: Southern Carnarvon Basin.||||||
25651|Wooramel Group|60295|5|Briefly described|p132|Artinskian|Sakmarian|Geological Province: Carnarvon Basin.||||||
25651|Wooramel Group|60331|5|Briefly described|p33 Fig.2|Artinskian|Artinskian|Overlain by Byro Group. Geological Province: Southern Carnarvon Basin.||||||
25651|Wooramel Group|60386|5|Briefly described|p297, 311|Artinskian|Artinskian|Carnarvon Basin. Proximal shelf.||||||
25651|Wooramel Group|60725|5|Briefly described|p29-32; p34-37; p39.|Early Permian|Early Permian|Merlinleigh Sub-basin. 380 m thick. Contains significant elements of a petroleum system. Fair to very good hydrocarbon source potential. Immature to marginally mature source beds.||||||10-MAY-17
25651|Wooramel Group|61023|5|Briefly described|p34 Fig. 14|Permian|Permian|Geological Province: Southern Carnarvon Basin.||||||11-APR-08
25651|Wooramel Group|61958|5|Briefly described|Map sheet 1|Artinskian|Artinskian|Includes 10 units: Cordalie Greywacke, Moogooloo Sandstone, Nunnery Sandstone, Monument Formation,  Jimba Jimba Calcarenite,  Curbur Formation,  Congo Formation,  One Gum Formation, Billidee Formation and  Keogh Formation.||||||
25651|Wooramel Group|62113|5|Briefly described|p628.|||Carnarvon Basin. This unit's lower coarse-grained sandstone facies is equivalent to the Irwin River Coal Measures.||||||
25651|Wooramel Group|64580|4|Described|map legend||Early Permian|Fine- to coarse-grained sandstone, siltstone, minor granule to pebble conglomerate.||||||09-DEC-08
25651|Wooramel Group|64630|5|Briefly described|p31 Fig.2, p35|Artinskian|Artinskian|Province: Southern Carnarvon Basin. Underlies the Byro Group, overlies the Callytharra Formation. Includes Billidee Formation at top. Palynology age: D. byroensis to M. trisina.||||||18-JAN-10
25651|Wooramel Group|64972|5|Briefly described|p615, p617 Fig. 4, p617 Fig. 5, p620|Early Permian|Early Permian|Includes Keogh Formation. Geological Province: Carnarvon Basin.||||||
25651|Wooramel Group|64974|6|Mentioned|p146, p147 Fig. 5|Artinskian|Artinskian|Geological Province: Carnarvon Basin.||||||24-JUN-09
25651|Wooramel Group|66189|6|Mentioned|p454, p455 Fig.2|Artinskian|Artinskian|Overlies the Callytharra Formation; is overlain by Byro Group. Marine sediments.||||||
25651|Wooramel Group|66579|5|Briefly described|Map legend|Permian|Permian|Southern Carnarvon Basin.|||Includes Moogooloo Sandstone and Billidee Formation.||Sandstones, siltstone, shale, conglomerate.|
25651|Wooramel Group|67200|5|Briefly described|p7 fig 5,|Kungurian|Artinskian||||Includes Billidee Formation, Moogooloo Sandstone, Keogh Formation, Cordalia Formation|Overlain by Byro Group||
25651|Wooramel Group|67373|5|Briefly described|Map legend.|Permian|Permian|Southern Carnarvon Basin.|||Includes Moogooloo Sandstone and Billidee Formation.|||
25651|Wooramel Group|67977|5|Briefly described|p479-80, p481 Fig. 2, p491|||Prograding fluvio-deltaic facies (Mory and Backhouse, 1997; Mory et al., 2003). Geol. Prov: Southern Carnarvon Basin.|||Keogh Formation, Billidee Formation and Moogooloo Sandstone|conformably overlies Callytharra Formation; is overlain by Byro Group||
25651|Wooramel Group|69011|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin.|||Includes the Moogooloo Sandstone and Billidee Formation.|Underlain by the Callytharra Formation. Overlain by the Byro Group.|Includes grey siltstone; fine- to medium-grained sandstone; fine to very coarse grained quartz sandstone; lesser black shale; minor granule to pebble conglomerate.|28-APR-14
25651|Wooramel Group|69028|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin.|||||Includes fine- to coarse-grained sandstone, siltstone, minor granule- to pebble-conglomerate.|
25651|Wooramel Group|69029|5|Briefly described|p313,323,326-328,333|Artinskian|Sakmarian|Of onshore Carnarvon Basin. Thickness: up to 380m. Contains interbedded organic-rich shales, with good to fair source potential and are dominantly gas-prone (up to 16% TOC, average 7% and potential yield up to 12mg/mg). Source rock potential decreases southward; mostly immature to early oil generative stage except on Kennedy-1 (overmature due to local intrusion).||||Overlain by Byro Group. Underlain by .||
25651|Wooramel Group|69166|5|Briefly described|500k_geologyp08_lut.csv|Artinskian|Artinskian||||Includes Billidee Formation, Moogooloo Sandstone||Fine to coarse grained sandstone, siltstone, minor granule to pebble conglomerate.|
25651|Wooramel Group|69182|6|Mentioned|Ch3 p3, Ch3 p8, Ch3 p10-p11|Permian|Permian|Carnarvon Basin. See also Ch3 p15, Ch3 p17-p20, Ch3 p23, Ch3 p35, Ch3 p37, Ch3 p67-p68, Ch3 p73. ||||Overlies the Lyons Group. Overlain by the Locker Shale.||
25651|Wooramel Group|69547|5|Briefly described|p182,193,195|Artinskian|Artinskian|Southern Carnarvon Basin.|||Includes Callytharra Formation.||Fluvial-marine sandstone.|
25651|Wooramel Group|69583|5|Briefly described|p130, Plate 3.|Permian|Permian|Southern Carnarvon Basin.|||||Undivided: fine- to coarse-grained sandstone, siltstone, and minor granule to pebble conglomerate.|
25651|Wooramel Group|70138|5|Briefly described|Map legend.|Permian|Permian|Southern Carnarvon Basin.|||Moogooloo Sandstone, Billidee Formation.|||
25651|Wooramel Group|70774|5|Briefly described|p5 fig 3|Artinskian|Artinskian|Southern Carnarvon Basin.||||Overlies the Callytharra Formation. Overlain by the Byro Group.||
25651|Wooramel Group|70795|4|Described|100k_geologyp_lut.csv|||Also 2_5m_interpgeop15_lut.csv|||Includes Billidee Formation, Moogooloo Sandstone||Fine to coarse grained sandstone, siltstone and minor granule to pebble conglomerate.|
25651|Wooramel Group|70826|6|Mentioned|p6 tbl 3|Permian|Permian|Southern Carnarvon Basin.||||||
25651|Wooramel Group|71146|5|Briefly described|p6|Artinskian|Sakmarian|Southern Carnarvon Basin.||||Overlies the Callytharra Formation. Overlain by the Byro Group.|Sandstone.|
25651|Wooramel Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone, greywacke|
25651|Wooramel Group|72034|5|Briefly described|500k_interpgeop16_lut|Artinskian|Sakmarian|Southern Carnarvon Basin.  Age from biostratigraphy.|||||Fine- to coarse-grained sandstone, siltstone, and minor granule to pebble conglomerate.|
25651|Wooramel Group|72505|5|Briefly described|p890|Kungurian|Artinskian|Southern Carnarvon Basin. Shown to correlate with the Microbaculispora trisina zone.||||Overlies the Callytharra Formation. Overlain by the Byro Group.||18-MAR-20
25651|Wooramel Group|72910|4|Described|p1, 4, 6, 11, 14, p17-18, p20, p22-24.|Artinskian|Artinskian|Occurs in Merlinleigh and Byro Sub-basins, Carnarvon Basin. Thickness 50-460m. Intersected  in Kennedy Range 1 well which contains a complete section of this group. Sparse macrofuana. See also p31, p38-39, p41-42. Formerly included Nunnery Sandstone, One Gum, Monument and Curbur Formations (Condon, 1967).|||Cordalia Formation, Moogooloo Sandstone, Keogh Formation, and Billidee Formation|Conformably underlies Byro Group and unconformably overlies Callytharra Formation and is partly laterally equivalent to Irwin River Coal Measures.|Fine to coarse-grained sandstone with minor conglomerate and siltstone.|18-FEB-21
25651|Wooramel Group|73117|6|Mentioned|p15|Artinskian|Artinskian|||||Underlain by Callytharra Formation. Overlain by Byro Group.||
25651|Wooramel Group|73623|5|Briefly described|p4|Cisuralian|Cisuralian|Merlinleigh Basin.||||Overlies Callytharra Formation. Is overlain by Byro Group. Correlative of Irwin River Coal Measures.||
24124|Worral Formation|13996|6|Mentioned|p128-129|Silurian|Silurian|Canning Basin. Contains Llandovery-aged conodonts (species named) which have affinities with European and North American sequences.||||||
24124|Worral Formation|14228|5|Briefly described|p6 fig3|Givetian|Emsian|South Canning Basin.||||Overlain by Tandalgoo Formation.||06-OCT-16
24124|Worral Formation|22753|5|Briefly described|Fig.3 p585|Devonian|Devonian|||||||
24124|Worral Formation|24449|5|Briefly described|p741 Fig. 2|Pridolian|Ludlovian|Age: ~425m.y.  Geological Province: Canning Basin.||||||
24124|Worral Formation|40837|2|Defined|2p58, p274|Emsian|Emsian|Overlies the Carribuddy Group. Type section: Barbwire No.1 drill core. See also Fig. 5 page insert (p258).||||||27-JAN-10
24124|Worral Formation|40992|6|Mentioned|Fig.11|||||||||
24124|Worral Formation|41169|6|Mentioned|p141|||||||||
24124|Worral Formation|41215|6|Mentioned|p262|||||||||
24124|Worral Formation|41913|6|Mentioned|Fig.2 p107|||||||||18-MAR-20
24124|Worral Formation|42030|5|Briefly described|p746|||||||||
24124|Worral Formation|42347|6|Mentioned|Fig.2 p1020|||||||||18-MAR-20
24124|Worral Formation|42880|5|Briefly described|Fig.2,p1020|||||||||
24124|Worral Formation|42933|5|Briefly described|Fig.94 p258|||||||||
24124|Worral Formation|43563|6|Mentioned|Fig.3,p7|Wenlock|Llandovery|||||||
24124|Worral Formation|43599|6|Mentioned|p247|||||||||
24124|Worral Formation|43656|6|Mentioned|Fig.2,p8|Givetian|Pragian|||||||
24124|Worral Formation|43666|6|Mentioned|p21|Eifelian|Emsian|||||||
24124|Worral Formation|43746|6|Mentioned|Fig.2, p11|Givetian|Emsian|||||||18-MAR-20
24124|Worral Formation|43818|6|Mentioned|Fig.2.p39||Early Devonian|||||||
24124|Worral Formation|44143|4|Described|p428, p440 Tb.4-19, p442, p443 Fig.4-98|Devonian|Devonian|Up to 200m thick; red-brown siltstone, sandstone and dolomite; marine and aeolian. Unconformably overlies Carribuddy Group. Type section between 457m and 613m in Barbwire 1 (CROSSLAND: 19deg 10' 38" S, 125deg 00' 59" E).||||||24-NOV-17
24124|Worral Formation|61021|5|Briefly described|p36 Fig. 2|Givetian|Emsian|Geological Province: Canning Basin.||||||17-DEC-07
24124|Worral Formation|61551|6|Mentioned|p351 Fig.2. |Givetian|Emsian|||||||
24124|Worral Formation|64643|5|Briefly described|p3 Fig. 2|Pridoli|Llandovery|||||||
24124|Worral Formation|64982|5|Briefly described|p699 Fig.4.|Llandovery|Llandovery|Up to 200 m thick aeolian to supratidal deposits. Local conodonts.||||Unconformably overlies Carribuddy Group. Is unconformably overlain by Tandalgoo Formation.|Red-brown siltstones, sandstones and dolomite.|
24124|Worral Formation|65214|6|Mentioned|p272, p277|Devonian|Devonian|QLD, Broken River and Canning Basin. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
24124|Worral Formation|65301|5|Briefly described|p3, p5 Fig. 4|Devonian|Llandovery|Contains the Elsa Sandstone Member. Conformably overlies Carribuddy Group; disconformably overlain by Tandalgoo Formation. Geological province: Canning Basin. Includes reservoir sandstones. Age: Llandovery - ?Devonian||||||23-FEB-10
24124|Worral Formation|65449|3|Fully described|p1, p3-11, p13-14, p21, p27-35, p38-40|Pridoli|Llandovery|See also p45-57; Plates 1-11. Canning Basin. Named after Worral Range. No outcrop. Lehmann (1984) separated the interval 2688-2571m in Kidson 1, previously within the Carribuddy Formation, as a new unit on the basis of an inferred regional angular stratigraphic break, and included it in the Tanndulla Group. Type section was 613-457m in Barbwire 1. Average thickness 140m. A regional seal to the prospective Larapintine 2 petroleum system. Has potential sandstone and carbonate reservoirs locally. Top of Megasequence I of Warris (1993). Regarded in this report as genetically more closely related to the Carribuddy Group than the Tandulla Group. These rocks were formerly included in the superseded Carribuddy Formation (now Carribuddy Group), but were separated on the basis of an inferred regional unconformity. Previous relationships are discussed. Details of petroleum wells/mineral drillholes intersecting this unit. Biostratigraphic data detailed.||Tanndulla Group.|Dodonea, Elsa Sandstone, and Waldecks Members.|Overlies Carribuddy Group. Is overlain by Tandalgoo Formation, probably unconformably. Correlated with Dirk Hartog Group (part).|Dominantly red-brown and lesser green and grey mudstone, in part calcareous and dolomitic; variable content of fine to medium, and less commonly coarse, grained sandstone; interbeds of dolomite and limestone; disseminated evaporites, esp. anhydrite.|
24124|Worral Formation|68007|4|Described|p1-2, p4, p6-7, p10, p12, p14-15|Early Devonian|Silurian|See also Plates 1, 2. Canning Basin. About 130m thick in Patience 2 well. Good to excellent reservoir potential. Composite well log.|||Includes Elsa Sandstone Member.|Overlies Sahara Formation (Carribuddy Group) conformably or paraconformably. Is overlain disconformably by Tandalgoo Formation.|Marginal marine carbonates and siltstone, with interbedded sandstone, some of which is considered aeolian.|24-FEB-20
24124|Worral Formation|68902|6|Mentioned|p9 fig 5|Silurian|Silurian|||||Overlies Sahara Formation.||
24124|Worral Formation|69029|6|Mentioned|p319|Givetian|Emsian|Of Canning Basin.||||Overlain by Tandalgoo Sandstone. Underlain by Sahara Formation.||
24124|Worral Formation|69182|5|Briefly described|Ch4 p9-p12, Ch4 p30-p36, Ch4 p38-p41|Lower Devonian|Llandovery|Canning Basin. This formation contains a number of potential seal horizons for the storage of carbon dioxide. Excellent potential as a carbon dioxide reservoir. See also Ch4 p44, Ch4 p45, Ch4 p47, Ch4 p50-p58, Ch4 p70, Ch4 p74, Ch4 p78-p82, Ch4 p86, Ch4 p92, Ch4 p94. |||Includes the Waldecks Member|Overlies the Sahara Formation and the Carribuddy Group. Overlain by the Tandalgoo Formation.|Red-bed claystones with minor carbonates.|
24124|Worral Formation|69312|5|Briefly described|p3, p23 fig 26|Pridoli|Wenlock|Canning Basin. See also p24 fig 28, p26 fig 32, p27 fig 34. ||||Overlies the Sahara Formation of the Carribuddy Group. Unconformably (or disconformably) overlain by the Tandalgoo Sandstone.|Shale.|
24124|Worral Formation|70774|5|Briefly described|p4|Pridoli|Llandovery|Willara and Kidson Sub-basins, Canning Basin.||||Overlies the Sahara Formation (Carribuddy Group). Unconformably? overlain by the Tandalgoo Formation.||
24124|Worral Formation|71146|5|Briefly described|p6, p29|Lochkovian|Llandovery|Canning Basin.||||Overlies the Carribuddy Group. Overlain by the Tandalgoo Formation.|Carbonate and mudstone.|
24124|Worral Formation|71870|5|Briefly described|p3|Givetian|Emsian|Canning Basin.||||Unconformably overlies the Sahara Formation.||
24124|Worral Formation|71894|5|Briefly described|p4|Lower Devonian|Llandovery|Canning Basin.||||Overlies the Sahara Formation (Carribuddy Group). Overlain by the Tandalgoo Formation.|Carbonate and shale.|
24124|Worral Formation|72497|5|Briefly described|p3 Fig.2.|Givetian|Emsian|Shown as occuring in the Jurgurra and Barbwire Terraces and Broome Platform.||||Conformably underlies Mellinjerie Formation. Laterally equivalent to Tandalgoo Formation. Unconformably overlies Sahara Formation.||
24124|Worral Formation|72499|5|Briefly described|p7 Fig.6.|Early Devonian|Llandovery|Located in the Willara Sub-basin and Broome Platform.||||Overlies Sahara Formation  and underlies Tandalgoo Formation.|Includes carbonate shales.|
24124|Worral Formation|72504|6|Mentioned|Figure 3|Devonian|Devonian|Canning Basin, Broome Platform. Intersected in Pictor 1, Sally May 2 drillholes, and possibly Fruitcake 1, Looma 1.||||||18-MAR-20
24124|Worral Formation|73117|5|Briefly described|p3, p31, p129, p141-142|Lower Devonian|Llandovery|Canning Basin. Local thickening in several wells assigned to this unit was reassessed by the authors as belonging to the Grant Group.||||Underlain by Cobb Formation and Carribuddy Group including Sahara Formation.|Dominantly carbonate-shale, marl.|
24124|Worral Formation|73346|6|Mentioned|p3, p25-26|Silurian|Late Ordovician|Canning Basin. Paralic.||||||
28140|Wungabal Limestone|13194|4|Described|p392 Tb. 4-16, p402 fig 4-66|Middle Famennian|Middle Famennian|Type Section: West of Tanmurra bore 15o06'S 128o38'E. Zero to 100m thick marginal slope facies.||Ningbing Group||Subsurface equivalent to and overlies (unconformably) Kamilili Formation.  Overlain by Garimala Limestone (unconformably).|Red "scheck" breccia and fossiliferous limestone.|
28140|Wungabal Limestone|40993|2|Defined|p8|Famennian|Famennian|||||||
28140|Wungabal Limestone|41864|3|Fully described|p92|||||||||
28140|Wungabal Limestone|41865|5|Briefly described|Map legend||middle Famennian|||||||
28140|Wungabal Limestone|41867|5|Briefly described|Map legend||middle Famennian|||||||
28140|Wungabal Limestone|42030|5|Briefly described|p750|||||||||
28140|Wungabal Limestone|64580|6|Mentioned|map legend|||||||||15-DEC-08
28140|Wungabal Limestone|64694|5|Briefly described|p234 Fig.2|Late Devonian|Late Devonian|Carlton Shelf, Onshore Bonaparte Basin.||Unit in Ningbing Group.||||
28140|Wungabal Limestone|69099|5|Briefly described|500k_geologyp08_lut.csv|Late Devonian|Late Devonian|||Ningbing Group||||
28140|Wungabal Limestone|69165|6|Mentioned|500k_geologyp08_lut.csv|Famennian|Frasnian|||||||
28140|Wungabal Limestone|69452|6|Mentioned|p36:7|||||Ningbing Group.||||12-JUL-16
28140|Wungabal Limestone|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Ningbing Group.||||
28140|Wungabal Limestone|69673|6|Mentioned|p169|||||Ningbing Group||Overlain by Garimala Limestone, overlies Kamilili Formation||
78357|Wurarga Granodiorite|69583|5|Briefly described|p49|Mesoarchean|Mesoarchean|Murchison Domain.||Bunnawarra Suite.||||
78357|Wurarga Granodiorite|69584|5|Briefly described|p5 Fig.2|Mesoarchean|Mesoarchean||c. 2950 Ma|Bunnawarra Suite|||Granodiorite.|
78357|Wurarga Granodiorite|69586|5|Briefly described|p22|Mesoarchean|Mesoarchean|Murchison Domain.||Bunnawarra Suite.||||
27020|Wururu Rhyolite|30388|4|Described|Table 1|||Middle Proterozoic age. See also P9,10||||||
27020|Wururu Rhyolite|30390|4|Described|p68|||||||||
27020|Wururu Rhyolite|30944|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27020|Wururu Rhyolite|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27020|Wururu Rhyolite|36551|6|Mentioned|Table 31|||||||||
27020|Wururu Rhyolite|36886|4|Described|p198|||||||||
27020|Wururu Rhyolite|67244|5|Briefly described|Map legend.|||Bentley Basin. Shown only in the Interpreted Bedrock Geology section of the map sheet.||Unit in Cassidy Group.|||Massive to flow-banded, porphyritic rhyolite.|11-APR-12
27020|Wururu Rhyolite|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Unit in Cassidy Group.|||Porphyritic rhyolite, massive to flow-banded.|
27020|Wururu Rhyolite|67375|5|Briefly described|p19 Fig.11, p38 Table 1. |Mesoproterozoic|Mesoproterozoic||1065 +/- 5 Ma.|Basal unit in Cassidy Group.||Overlies Glyde Formation. Is overlain by Gombugurra Rhyolite or Gurgadi Basalt.|Dark-grey, feldspar-phyric rhyolite with very fine-grained groundmass; massive, flow-banded or spherulitic.|
27020|Wururu Rhyolite|67553|4|Described|p20-21,40,44,50-51,53|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Talbot Sub-basin, Bentley Sub-basin. Crystallisation age at 1065+\-5 Ma (GSWA 174690), coeval with deposition of upper section of Mount Palgrave Group. Defines the base of the Cassidy Group, and top of the Pussy Cat Group.|1065+\-5 Ma|Unit of Cassidy Group.||Lowermost unit of Cassidy Group. Overlain by Gombugurra Rhyolite. Underlain by Glyde Formation/Pussy Cat Group.||
27020|Wururu Rhyolite|68995|6|Mentioned|p7 Fig.3, p9 Tb.1, p15, p18, p22|Stenian|Stenian|Estimated 810m thick. Between this unit and the Gombugurra Rhyolite is an unnamed unit of sedimentary rocks that is approximately 50m thick and composed of fine grained siltstone with layers of sandstone and conglomerate and very minor layers of basalt. Metamorphism discussed. See also p27 Tb.2, p56.||Cassidy Group||Overlain by the Gombugurra Rhyolite.|Rhyolitic lava flows or rheomorphic ignimbrites.|
27020|Wururu Rhyolite|69091|5|Briefly described|p71 Fig.4.14|||Talbot Sub-basin||Cassidy Group||||
27020|Wururu Rhyolite|69153|6|Mentioned|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen. Geochron analysis is interpreted as magmatic crystallization age (GEOCHRON/174690.1.pdf). Also mentioned in GEOCHRON/174691.1.pdf. ||Cassidy Group|||Porphyritic rhyolite|24-MAR-16
27020|Wururu Rhyolite|69729|6|Mentioned|p82|||Bedrock of Talbot Sub-basin.||Cassidy Group.||||
27020|Wururu Rhyolite|70095|5|Briefly described|p16-17,19,21|||Geological province: Musgrave Province. Talbot Sub-basin, Of Bentley Basin. Thickness of rhyolitic package: 0.81km, over 74km in strike length and Interpreted minimum volume of 1800 km3 (potentially reflecting up to three separate volumes). Generally characteristed by highly depleted 18O isotopes. See p19 Table 2 for U-Pb zircon data. See p21 Table 3 for SIMS oxygen isotope data.||Unit of Cassidy Group.||Lowermost unit of Cassidy Group. Overlain by Gombugurra Rhyolite. Underlain by Pussy Cat Group.||
27020|Wururu Rhyolite|70134|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|c.1065 Ma.|Cassidy Group.||Is overlain by Gombugurra Rhyolite.|Porphyritic rhyolite, massive to flow-banded.|
27020|Wururu Rhyolite|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|c.1065 Ma.|Cassidy Group.||Overlies Glyde Formation. Is overlain by Gombugurra Rhyolite.|Porphyritic rhyolite, massive to flow-banded.|
27020|Wururu Rhyolite|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|SHRIMP age obtained from rhyolite sample (file 17490.1.pdf)|1047 Ma - 1077 Ma (Inferred) 1065 Ma (SHRIMP)|Cassidy Group|||Porphyritic rhyolite; massive to flow banded|
27020|Wururu Rhyolite|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Sample GSWA 174690 (rhyolite) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) magmatic crystallisation age of 1065+\-5 Ma. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv.|1077-1047 Ma (inferred)|Unit of Cassidy Group.|||Porphyritic rhyolite; massive to flow banded|
27020|Wururu Rhyolite|71211|6|Mentioned|p216|||||Cassidy Group||||
27020|Wururu Rhyolite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Sample GSWA 174690 (rhyolite) yielded a concordia age of 1065+\-5 Ma, interpreted as the magmatic crystallization age of the rhyolite. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv.|1077-1047 Ma (inferred)|Unit of Cassidy Group.|||Porphyritic rhyolite; massive to flow banded|
27020|Wururu Rhyolite|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1065+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite.|
27020|Wururu Rhyolite|72443|6|Mentioned|p738-739, p742, p747|||Talbot Sub-basin.|1033 +/- 24 to 1066 +/- 8 Ma (SHRIMP U-Pb)|Cassidy Group||||
33835|Wyloo Supersequence|22546|4|Described|370||Paleoproterozoic|Geol province Wyloo Basin. Estimated age 2000 Ma||||||07-NOV-08
33835|Wyloo Supersequence|22682|5|Briefly described|Fig21,p31|Orosirian|Orosirian|2044-1997 Ma. Ashburton Province||||||
26238|Wyman Formation|22715|5|Briefly described|table7 p214|Archean|Archean|Age: 3325Ma||||||07-NOV-08
26238|Wyman Formation|22727|6|Mentioned|p635,8||Archean|||||||07-NOV-08
26238|Wyman Formation|23046|5|Briefly described|169|||||||||
26238|Wyman Formation|23134|5|Briefly described|p288|||||||||
26238|Wyman Formation|23206|6|Mentioned|Fig.1|||Age: 3.32Ga.||||||
26238|Wyman Formation|23244|6|Mentioned|Table.1|||||||||
26238|Wyman Formation|23255|5|Briefly described|p48 Fig.2||Archean|Age: 3325+/-4Ma.||||||07-NOV-08
26238|Wyman Formation|23755|5|Briefly described|p8|Archean|Archean|Age: 3325+/-4 Ma.||||||07-NOV-08
26238|Wyman Formation|23780|5|Briefly described|p133|Archean|Archean|||||||07-NOV-08
26238|Wyman Formation|23783|4|Described|p15|Archean|Archean|Age: 3325-3308Ma. Max Thickness: 1100m.||||||07-NOV-08
26238|Wyman Formation|23784|5|Briefly described|p2|Archean|Archean|Age: 3330-3310Ma.||||||07-NOV-08
26238|Wyman Formation|23807|5|Briefly described|p110|Archean|Archean|Age: 3325-3315Ma (SHRIMP).  Geological Province: Pilbara Craton.||||||07-NOV-08
26238|Wyman Formation|23813|5|Briefly described|p103|Archean|Archean|Potassic rhyolites.  Age: 3325-3315Ma.  Geological Province: Pilbara Craton.  See also p91 Tb. 1||||||07-NOV-08
26238|Wyman Formation|23891|5|Briefly described|p89|Archean|Archean|Of Mount Bruce Supsergroup.Calc-alkaline rocks. Igneous age: ~3315Ma. Geological Province: Pilbara Craton.  See also p98.||||||07-NOV-08
26238|Wyman Formation|23895|5|Briefly described|p885 Fig.2|||||||||
26238|Wyman Formation|23936|4|Described|p2|Archean|Archean|Age: ca. 3325-3307 Ma. Geological Province: Pilbara Craton. Underlain by Warrawoona Group ( unconformably).||||||07-NOV-08
26238|Wyman Formation|24025|4|Described|p8 Tb. 1|Archean|Archean|Rhyolite, felsic pyroclastic rocks and debris-flow deposits; local chert and basalt.  Age: c.3325Ma.  Geological Province: Pilbara Craton. Max Thickness: 1000m.||||||07-NOV-08
26238|Wyman Formation|24110|5|Briefly described|Plate 1|Archean|Archean|Of the Pilbara Supergroup. Geological Province: Pilbara Craton||||||07-NOV-08
26238|Wyman Formation|24184|4|Described|p699, 701|Archean|Archean|Of the Kelly Subgroup. Overlain by Charteris Basalt. Geological Province: Pilbara Craton. Max Thickness: 1100m. Age: ca.3325-3312Ma. Formerly of the Warrawoona Group (Hickman 1990), now placed together with Euro Basalt in the new Kelly Subgroup.||||||07-NOV-08
26238|Wyman Formation|24185|5|Briefly described|p734, p737 Tb.2|Archean|Archean|Age: ca. 3325-3308 Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
26238|Wyman Formation|24531|5|Briefly described|p5|Archean|Archean|Of the Kelly Subgroup (Warrawoona Group).  Age: c.3325-3319Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
26238|Wyman Formation|24550|5|Briefly described|p31 Tb. 3.1|Archean|Archean|Of the Kelly Subgroup (Warrawoona Group). Felsic volcanics. Age: 3325Ma. Max. thickness: 1.1km. Geological Province: Pilbara Craton.||||||07-FEB-11
26238|Wyman Formation|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Of the newly formed Kelly Subgroup, together with Euro Basalt. Felsic volcanic rocks. Unconformably overlies the Duffer Formation and Salgash Subgroup ; unconformably overlain by Gorge Creek Group.  Age: 3325-3315Ma.||||||07-FEB-11
26238|Wyman Formation|30766|4|Described|p13|||Refers Hickman and Lipple (1975).||||||24-JUL-07
26238|Wyman Formation|31309|6|Mentioned|Table 8|||refs Lipple 1975||||||
26238|Wyman Formation|31853|2|Defined|p61|Archean|Archean|||||||07-NOV-08
26238|Wyman Formation|34829|6|Mentioned|Fig.2|||||||||
26238|Wyman Formation|35142|6|Mentioned|Fig.1|||||||||
26238|Wyman Formation|35531|6|Mentioned|Fig.1|||Composite lithostratigraphic section||||||
26238|Wyman Formation|37373|4|Described|p79|||||||||
26238|Wyman Formation|37899|6|Mentioned|Fig.2|||||||||
26238|Wyman Formation|38242|6|Mentioned|Fig.1|||||||||
26238|Wyman Formation|38481|5|Briefly described|p267|||||||||
26238|Wyman Formation|38498|5|Briefly described|Table 1|||||||||
26238|Wyman Formation|38544|6|Mentioned|Fig.1|||||||||
26238|Wyman Formation|38624|6|Mentioned|Fig.2|||||||||
26238|Wyman Formation|38763|6|Mentioned|Table 3|||||||||
26238|Wyman Formation|39426|6|Mentioned|Fig.3|||||||||
26238|Wyman Formation|39444|6|Mentioned|Table 1|||||||||
26238|Wyman Formation|39559|6|Mentioned|Table 1|||||||||
26238|Wyman Formation|39580|4|Described|p293|||||||||
26238|Wyman Formation|39672|6|Mentioned|p241|||||||||
26238|Wyman Formation|39697|3|Fully described|p96|||||||||
26238|Wyman Formation|40596|6|Mentioned|p67|||Mention Fig.1||||||
26238|Wyman Formation|41349|6|Mentioned|p4|||||||||
26238|Wyman Formation|41350|6|Mentioned|p25|||||||||
26238|Wyman Formation|41636|6|Mentioned|p79|||||||||
26238|Wyman Formation|43052|5|Briefly described|Fig.3.8|||||||||
26238|Wyman Formation|43595|5|Briefly described|p213|||||||||
26238|Wyman Formation|43698|6|Mentioned|p26|||||||||
26238|Wyman Formation|43769|6|Mentioned|Fig.3,p858|||3.325 Ga||||||
26238|Wyman Formation|44150|5|Briefly described|p129 Tb.2-15, p132-134, p138, p140|||See also p152 Tb.2-22, p155, p157 Fig.2-144. 0 - 1 km thick.||Warrawoona Group||Overlies Salgash Subgroup, partly unconformably.|Metamorphosed porphyritic, columnar-jointed rhyolite; local tuff, agglomerate and basalt.|
26238|Wyman Formation|46319|5|Briefly described|p6 Fig. 3|Archean|Archean|Of Warrawoona Group.  Geological Province: Pilbara Craton.||||||07-NOV-08
26238|Wyman Formation|50381|5|Briefly described|Map Legend|Archean|Archean|Of Kelly Subgroup (Warrawoona Group). Geological Province: Pilbara Craton.||||||07-NOV-08
26238|Wyman Formation|50423|4|Described|p216||Archean|Age: 3325-3315 Ma. Felsic volcanics. Of upper Warrawoona Group.||||||07-NOV-08
26238|Wyman Formation|50427|5|Briefly described|p185 Fig.7, p192 Fig.11|Archean|Archean|Age: 3325-3315 Ma. Conformably overlies Warrrawoona Group. Unconformably overlain by Budjan Creek Formation.||||||07-NOV-08
26238|Wyman Formation|50544|6|Mentioned|p39|Archean|Archean|Granitoid dome.  Age: c.3325-3320Ma.  Not on the YARRIE sheet.||||||07-NOV-08
26238|Wyman Formation|60112|6|Mentioned|p107 Fig.1. |||||||||
26238|Wyman Formation|60636|5|Briefly described|p35-36 Fig. 3.2, p44|||Of the Warrawoona Group. Includes the previous 'P-assemblage' (feldspar porphyry) of the Panorama Formation. Presented as Wyman only in text of figure.||||||07-FEB-11
26238|Wyman Formation|61253|5|Briefly described|p51, p52 Fig. 2|Archean|Archean|Of the Kelly Group (Pilbara Supergroup).  Geological Province: Pilbara Craton.||||||07-NOV-08
26238|Wyman Formation|61264|5|Briefly described|p64 Fig. 2|||Of the Kelly Group (Pilbara Supergroup). Geological Province: East Pilbara Granite-Greenstone Terrane/Pilbara Craton.||||||
26238|Wyman Formation|62427|5|Briefly described|p3 Fig.2, p4, p6 |Paleoarchean|Paleoarchean||3318 +/- 4 Ma (U-Pb zircon).|Of the Warrawoona Group.||||
26238|Wyman Formation|63245|5|Briefly described|p5 Fig. 2|Archean|Archean|Of the Kelly Group (Pilbara Supergroup).  Age: 3325-3315Ma. Geological Province: Pilbara Craton. Felsic volcanics.||||||07-NOV-08
26238|Wyman Formation|63417|5|Briefly described|Map legend|Archean|Archean|Of the Kelly Group (Pilbara Supergroup). Age: 3325-3315Ma. Geological Province: Pilbara Craton. Felsic volcanic rock; local basalt; metamorphosed.||||||07-NOV-08
26238|Wyman Formation|63420|5|Briefly described|Map legend|Archean|Archean|Of Kelly Group (Pilbara Supergroup). Geological Province: Pilbara Craton. Felsic volcanic sandstone; tuffaceous; local quartz sandstone; metamorphosed.||||||07-NOV-08
26238|Wyman Formation|63441|5|Briefly described|p4 Tb. 1|Archean|Archean|Of the Kelly Group (Pilbara Supergroup).||||||07-FEB-11
26238|Wyman Formation|63538|4|Described|p3 Fig. 2, p5, p6 Fig. 3|Archean|Archean|Of Kelly Group. Overlain by Charteris Basalt, underlain by Euro Basalt. Age: c. 3325-3315 Ma. Geological Province: Pilbara Craton. Voluminous, high-K2O felsic volcanism.||||||19-APR-13
26238|Wyman Formation|63649|5|Briefly described|p201 Fig. 2|Archean|Archean|Of the Kelly Group. Age: 3.325 - 3.315Ga. Geological Province: Pilbara Craton.||||||07-FEB-11
26238|Wyman Formation|63854|5|Briefly described|p229 Fig.2 |||||Of the Kelly Group.||||
26238|Wyman Formation|64327|5|Briefly described|p63|Archean|Archean|Age: c.3325Ma.||||||07-NOV-08
26238|Wyman Formation|64328|4|Described|p54, p57|Archean|Archean|Of Kelly Subgroup (Warrawoona Gp). Age: c.3325-3320Ma. Thickness: ~1km. Conformably overlies Euro Basalt. Includes felsic volcanic rocks and sandstone. Excluded from Warrawoona Group until recent mapping established its inclusion. Lith.details included||||||07-FEB-11
26238|Wyman Formation|64405|5|Briefly described|p4 Fig. 3|Archean|Archean|Name inferred from Wyman only in Figure 3. Of the Kelly Group (De Grey Supergroup).Felsic rocks.||||||07-FEB-11
26238|Wyman Formation|64580|4|Described|map legend||Paleoarchean|Of Kelly Group. Felsic volcanic and volcaniclastic rocks; local clastic sedimentary rocks, chert and basalt; metamorphosed.||||||09-DEC-08
26238|Wyman Formation|64621|5|Briefly described|Map legend|Archean|Archean|Of the Kelly Group ( Pilbara Supergroup). Age: 3325-3315Ma. Comprehensive lithological details included.||||||07-NOV-08
26238|Wyman Formation|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Kelly Subgroup. Geological Province: Pilbara Craton. Fine-grained to porphyritic rhyolite and rhyodacite flows and agglomerates; metamorphosed. Medium-grained dolerite and local gabbro; metamorphosed, and chert.||||||07-FEB-11
26238|Wyman Formation|64747|6|Mentioned|p94 fig 1|||||||||
26238|Wyman Formation|64936|5|Briefly described|map legend|Archean|Archean|Of Kelly Subgroup. Age: 3325-3315 Ma (geochron: R Buick etal 2002; NJ McNaughton etal 1993; RI Thorpe etal 1992; DR Nelson 2001). Felsic tuff, volcaniclastic sandstone, quartz arenite. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
26238|Wyman Formation|65008|4|Described|p5, p7-12, p14, p15, p20, p41|Paleoarchean|Paleoarchean|East Pilbara Granite-Greenstone Terrane. Geochronology by: Nelson(2002). Includes 7 separately mapped facies. Redefined by Bagas et al. (2004a) as included in the Kelly Subgroup. ~1km thick. Intruded by the Boobina Porphyry.|3325-3319 Ma|Of the Kelly Subgroup||Conformably underlain by the Euro Basalt. Conformably overlain by the Charteris Basalt. Unconformably overlain by the Budjan Creek Formation, Gorge Creek Group, Corboy Formation, and Fortescue Group.|Fine-grained to porphyritic rhyolite and rhyodacite flows and agglomerate; basalt, massive and pillowed; finely layered chert and felsic tuff and schist, locally sheared; silstone, sandstone, and minor conglomerate, chert. All metamorphosed.|
26238|Wyman Formation|65415|6|Mentioned|p120 Fig.2.|Archean|Archean|||Unit in Pilbara Supergroup.||Unconformably overlies Warrawoona Group. Is overlain unconformably by Gorge Creek Group.||
26238|Wyman Formation|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton. Mapped as five sub-units.|c.3315 Ma (Nelson 2002).|Of Kelly Subgroup.|||Fine-grained to porphyritic rhyolite and rhyodacite flows and agglomerate; felsic agglomerate and tuff; interbedded siltstone and chert, minor carbonaceous pelite; chert; all metamorphosed.|
26238|Wyman Formation|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Mapped as four sub-units.|c.3325 - 3315 Ma (Barley and Pickard 1999).|Of Kelly Group.|||Porphyritic rhyolite and rhyodacite; felsic volcaniclastic rocks including debris-flow deposits, autobreccia and tuff; felsic volcanic sandstone interbedded with siltstone, chert, carbonaceous mudstone and basalt; chert. All metamorphosed.|
26238|Wyman Formation|65825|4|Described|p5, p6, pp9-10, p32.|Archean|Archean|Four un-named sub-units with differing lithologies are mapped separately and decribed in detail in the report. Re-assigned by Van Kranendonk et al. (2004) to the Kelly Group.||Unit in Kelly Group; formerly in Warrawoona Group.||Is overlain conformably by Warrawoona Group; unconformably by Mosquito Creek Formation and Fortescue Group; and in faulted contact with Coondamar Formation.|Metamorphosed, silicified clastic sedimentary rocks: mudstone, sandy siltstone, sandstone and chert-pebble sandstone; subordinate komatiitic basalt, commonly silicified, and gabbro; thin bands of chert and very minor amounts of ultramafic rock.|
26238|Wyman Formation|65827|3|Fully described|p6 Tb.1, p12 Tb.3, p13 Tb.4, p21-22, p28|Paleoarchean|Paleoarchean|Of Kelly Group; formerly of Kelly Subgroup. Eruptions 3325-3315 Ma. Dated 3315 +/- 3 (SHRIMP U-Pb zircon; Nelson 2002). Underlies Charteris Basalt conformably; unconformably underlies Gorge Creek Group, Farrel Quartzite, Fortescue Group, Mount Roe Basalt; conformably overlies Euro Basalt; intruded by Dalton Suite. Metamorphosed felsic volcaniclastic rocks: volcanic breccia, tuffaceous rocks, porphyritic rhyolite and rare rhyodacite; felsic volcanic sandstone with finer-grained interbeds; banded chert.||||||
26238|Wyman Formation|65828|5|Briefly described|Map legend|Archean|Archean|||Unit in Warrawoona Group.|||Massive and pillow basalt; grey chert and silicified rock of uncertain origin; siltstone, sandstone and minor conglomerate, typically silicified; gabbro and dolerite; all metamorphosed.|
26238|Wyman Formation|65829|6|Mentioned|p9, p13. |Paleoarchean|Paleoarchean||c.3315 Ma.|Unit in Kelly Group.||Overlies Euro Basalt.||
26238|Wyman Formation|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Kelly Group. Age shown as 3325-3315 Ma. Felsic volcanic and volcaniclastic rocks; local clastic sedimentary rocks, chert, and basalt; metamorphosed.||||||
26238|Wyman Formation|66217|4|Described|p5, p14, pp29-31, pp59-60.|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Van Kranendonk et al. (2002) included this unit in the Kelly Subgroup in their redefinition of the Warrawoona Group. Derived from melting of older felsic crust. Eruption was contemporaneous with emplacement of the Emu Pool Supersuite. Apparently the source of native sulfur crystals and white sulfate crusts in a Pear Creeek tributary.|3325-3315 Ma.|Unit in Kelly Group.||Is overlain conformably by Charteris Basalt, and unconformably by Sulphur Springs, Gorge Creek (Farrel Quartzite), Croydon and Fortescue Groups.|Weakly metamorphosed high-K rhyolitic flows and volcaniclastic rocks, pillowed komatiitic basalt, and minor chert.|
26238|Wyman Formation|66745|3|Fully described|p53 Fig.3, p54 Fig.4.|Paleoarchean|Paleoarchean|Hydrothermal activity, including shallow-water environments (stromatolites). Base metal mineralization.|3325-3315 Ma.|Unit in Kelly Group.||Overlies Euro Basalt. Is overlain by Charteris Basalt.|Felsic volcanic rocks, basalt.|
26238|Wyman Formation|67130|5|Briefly described|p16, p20 fig 13, p45|Paleoarchean|Paleoarchean||3325 Ma|||Overlies Euro Basalt, conformably overlain by Charteris Basalt|High K rhyolites.|
26238|Wyman Formation|67197|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.|3325-3310 Ma.|Kelly Group.||||
26238|Wyman Formation|67201|5|Briefly described|p7 Fig.4, p12 Tb.1|||In northern Pilbara Craton, East Pilbara Terrane.|c. 3320 Ma|Kelly Group||||
26238|Wyman Formation|67269|5|Briefly described|p6 Fig.3|Paleoarchean|Paleoarchean||3325-3315 Ma.|Kelly Group.||Overlies Euro Basalt. Is overlain by Charteris Basalt.||
26238|Wyman Formation|67270|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.|3325-3315 Ma.|Kelly Group.||||
26238|Wyman Formation|67668|6|Mentioned|Fig. 2; p. 154||Paleoarchean|East Pilbara Terrane, Pilbara Craton. Mis-spelled as Wyman Formations on p154.|3325 - 3315 Ma.|Kelly Group||Overlies the Euro Basalt, underlies the Charteris Basalt.||
26238|Wyman Formation|68035|4|Described|p288 Fig 4|Paleoarchean|Paleoarchean|Pilbara Supergroup, East Pilbara Terrane.|3325 - 3315 Ma|Of Kelly Group.||Overlies Euro Basalt. Overlain by Charteris Basalt.|Felsic volcanics, basalt, minor chert, siliciclastic rocks.|
26238|Wyman Formation|68280|5|Briefly described|p4||||3325-3315 Ma|Kelly Group||Overlies Euro Basalt, overlain by Charteris Basalt|Felsic volcanic rocks, basalt, chert and siliciclastic rocks.|18-JAN-23
26238|Wyman Formation|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Detailed lithology discussed in map legend; the 5 facies are mapped separately.|3325-3315 Ma|Of the Kelly Group.|||Massive and pillowed basalt; porphyritic rhyolite and rhyodacite; black chert and chert breccia; quartz sandstone; sandstone and chert pebble conglomerate; all metamorphosed.|
26238|Wyman Formation|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c.3325-3312 Ma (McNaughton et al. 1993).|Of the Kelly Group.|||Felsic volcanic sandstone; tuffaceous; local quartz sandstone; metamorphosed|
26238|Wyman Formation|68284|5|Briefly described|p4, 7|Paleoarchean|Paleoarchean|Crops out in the Marble Bar-Nullagine area, East Pilbara Terrane.|3325-3315 Ma.|Kelly Group.||Conformably overlies Euro Basalt. Is overlain by Charteris Basalt.|Felsic volcanic rocks and volcaniclastic sedimentary rocks.|
26238|Wyman Formation|69012|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane. Ten facies are mapped separately.|3325-3315 Ma (McNaughton et al., 1993)|Of the Kelly Group.|||Porphyritic rhyolite and rhyodacite; felsic volcanic breccia and sandstone; quartz sandstone; ferruginous shale; banded iron-formation; chert in hydrothermal veins; felsic schist; interlayered psammitic and pelitic rocks; all metamorphosed.|29-APR-14
26238|Wyman Formation|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Banded iron formation and ferruginous shale and chert. Porphyritic rhyolite and rhyodacite, pillowed basalt and komatiitic basalt. Ages derived from rhyolite and volcaniclastic sandstone samples(where it is the age of the volcanic component of the protolith) (160220.1.pdf, 169000.1.pdf)|3318 +/- 4 Ma - 3312 +/- 4 Ma(SHRIMP)|Kelly Group|||Interlayered psammitic and pelitic schists; metamorphosed shale, sandstone, quartz sandstone, lithic arenite, silstone, and conglomerate. Felsic schist, felsic volcanic sandstone, siltstone,breccia, chert and chert breccia in hydrothermal veins.|
26238|Wyman Formation|69185|4|Described|GEOL_LUT_CSV files||Paleoarchean|Geological province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 3325 Ma|Unit of Kelly Group.|||Felsic volcanic and volcaniclastic rocks; local clastic sedimentary rocks, chert and basalt; metamorphosed|
26238|Wyman Formation|69301|4|Described|p5 Fig.3, p9 Tb.1, p20 Tb.2|||Pilbara Craton. East Pilbara Terrane. Pilbara Supergroup successions include thick felsic volcanic formations, each contemporaneous with the four granitic supersuites. i.e. Wyman Formation and Emu Pool Supersuite.|3325-3315 Ma; 3320 Ma|Kelly Group|||Felsic volcanic rocks, basalt.|
26238|Wyman Formation|69566|5|Briefly described|p236-237|||East Pilbara Granite-Greenstone Terrane.|3315 +/- 5 Ma (Pidgeon, 1978).|Kelly Group.||Overlies Euro Basalt. Is overlain conformably by Charteris Basalt.|Felsic.|
26238|Wyman Formation|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA 144681 (agglomeratic rhyolite) yielded an interpreted igneous crystallisation age of 3315+\-3 Ma for the rhyolite (weighted mean 207Pb/206Pb). Sample GSWA 160218 (porphyritic dacite) yielded a preferred interpreted igneous crystallisation age of 3303+\-15 Ma for the dacite (weighted mean 207Pb/206Pb); alternate age includes a maximum eruptive age of 3248+\-7 Ma (youngest 207Pb/206Pb). Sample GSWA 160220 (tuffaceous rhyolite) yielded an interpreted igneous crystallisation age of 3318+\-15 Ma for the rhyolite (weighted mean 207Pb/206Pb). Sample GSWA 168910 (dacitic volcanic rock) yielded an interpreted igneous crystallisation age of 3323+\-3 Ma for the dacite (weighted mean 207Pb/206Pb). Sample GSWA 168992 (volcaniclastic metasandstone) yielded an interpreted maximum depositional age of 3324+\-4 Ma for the sedimentary protolith (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|3325-3315 Ma (inferred)|Unit of Kelly Group.|||Banded iron-formation, ferruginous shale; chert and chert breccia, felsic schist, felsic-volcanic- breccia, -sandstone and -siltstone, basalt; massive and pillowed, komatiitic; sandstone, siltstone, chert pebble conglomerate, rhyolite, rhyodacite.|
26238|Wyman Formation|70022|6|Mentioned|p113, 115-116, 118|||Warralong Greenstone Belt, East Pilbara Terrane.|~3.30 Ga.|Kelly Group.|||Volcaniclastic sandstone interstratified with rhyolites.|
26238|Wyman Formation|70775|5|Briefly described|p12|Paleoarchean|Paleoarchean|East Pilbara.|c. 3320 Ma|Kelly Group||Overlies the Euro Basalt. Overlain by the Charteris Basalt.||
26238|Wyman Formation|70884|5|Briefly described|p123,135|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|3.33-3.32 Ga|Unit of Kelly Group.||Overlain by Charteris Basalt. Underlain by Euro Basalt. Unconformably overlain by the Budjan Creek Formation.||16-AUG-19
26238|Wyman Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Kelly Large Igneous Province, East Pilbara Terrane.|Max age 3325+/-4 Ma, min 3215+/-3 Ma.|Kelly Group|||Felsic volcanic and volcaniclastic rocks; local clastic sedimentary rocks, chert and basalt; metamorphosed.|
26238|Wyman Formation|72064|5|Briefly described|p66|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Kelly Group.||Overlain by Charteris Basalt. Underlain by Euro Basalt.||
26238|Wyman Formation|72251|5|Briefly described|p54|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Kelly Group.||Overlain by Charteris Basalt. Underlain by Euro Basalt.||
26238|Wyman Formation|72668|5|Briefly described|p4-6, p8-9, p19-20, p24, p27|||East Pilbara Terrane. Genetically related to the Emu Pool Supersuite. Structure is discussed.|c. 3320-3310 Ma|Kelly Group||Overlies the Euro Basalt. Conformably overlain by the Charteris Basalt.|Rhyolitic volcanics.|14-JAN-22
26238|Wyman Formation|73598|6|Mentioned|p1212-12213|Paleoarchean|Paleoarchean|East Pilbara Terrane. Coeval with Kelly Dyke swarm.||Kelly Group.||Overlies Euro Basalt. Is overlain by Charteris Basalt.|Felsic volcanics.|
31959|Yabbat Granite|24197|6|Mentioned|p71 Tb. 7.1|||Of the Minnie Creek Supersuite.||||||07-FEB-11
31959|Yabbat Granite|50425|5|Briefly described|p1.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Province. Of the Minnie Creek Supersuite.||||||07-NOV-08
38137|Yadgimurrin Member|23529|6|Mentioned|p11 Fig. 5|||Of the Yelma Formation??||||||
38137|Yadgimurrin Member|24017|5|Briefly described|p12 Fig. 5|||Of the Yelma Formation.||||||07-AUG-08
38137|Yadgimurrin Member|50188|5|Briefly described|p4 Fig. 2|||Of the Yelma Formation. Geological Province: Earaheedy Basin.||||||16-JUL-08
38137|Yadgimurrin Member|50195|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Yelma Formation (Tooloo Subgroup, Earaheedy Group).  Geological Province: Earaheedy Basin.||||||07-NOV-08
38137|Yadgimurrin Member|50626|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Yelma Formation (Earaheedy Group).  Polymictic conglomerate.  Geological Province: Earaheedy Basin.||||||07-NOV-08
38137|Yadgimurrin Member|64284|5|Briefly described|p60 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of Yelma Formation (Tooloo Subgroup). Geological Province: Earaheedy Basin.||||||07-FEB-11
38137|Yadgimurrin Member|64772|4|Described|p9, p10 Fig. 5|Paleoproterozoic|Paleoproterozoic|Basal member of Yelma Fm (Earaheedy Gp). Not shown in Plate 1. Localised conglom. mbr. consisting of >100m boulder conglom. with clasts up to 1m across of granite, quartzite+chert in an arkosic matrix; + assoc'd pods/veins of jasperoidal chert, quartz.||||||07-FEB-11
38137|Yadgimurrin Member|65692|6|Mentioned|p56|||||Yelma Formation.||||
38137|Yadgimurrin Member|66427|5|Briefly described|p46 Fig.4, p51-52 |||Western Earaheedy Basin. Mis-spelt as Yadgimurin on p51. Some clasts sourced from underlying Mooloogool Group.||Of the Yelma Formation.|||Localised very coarse, poorly sorted conglomeratic unit with sandstone lenses, about 100m thick.|
38137|Yadgimurrin Member|69152|5|Briefly described|1m_geologyp08_lut.csv|Orosirian|Orosirian||||||Quartz sandstone, matrix-supported polymictic conglomerate, minor pebble conglomerate.|07-AUG-15
38137|Yadgimurrin Member|69313|6|Mentioned|p25 Fig.4.3|||||Yelma Formation||||
38137|Yadgimurrin Member|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, conglomerate|
38137|Yadgimurrin Member|71270|5|Briefly described|1m_geologyp12_lut.csv|||Geological province: Capricorn Orogen. Of Earaheedy Basin. ||Unit of Yelma Formation.|||Quartz sandstone, matrix-supported polymictic conglomerate, minor pebble conglomerate|
78532|Yalca Hill Monzogranite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||3010 - 2600 Ma (inferred).||||Biotite-bearing monzogranite.|
78532|Yalca Hill Monzogranite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2680 Ma (inferred)||||Biotite-bearing monzogranite|
78991|Yalgoo Formation|70226|5|Briefly described|Map legend.|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Carton.|2800-2735 Ma.|Polelle Group.|Yilgaddy Andesite Member, Singleton Basalt Member, Carlaminda Komatiite Member, Mugs Luck Basalt Member||Andesite, basalt, komatiite.|16-DEC-15
78991|Yalgoo Formation|70796|5|Briefly described|100k_geologyl_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 207686.1.pdf, Yalgoo100_2241_stratig.pdf.|ca 2790  2760 Ma (inferred)|Polelle Group|Includes the Yilgaddy Andesite Member, Singleton Basalt Member, Carlaminda Komatiite Member and the Mugs Luck Basalt Member.|||
78991|Yalgoo Formation|70830|5|Briefly described|p57|||Murchison Domain.|||Includes the Singleton Basalt Member.|||
78991|Yalgoo Formation|71269|4|Described|GEOL_LUT_CSV files + geochron files|||Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Lu et al. (2016a) dated a sample of metadacite at 2813+\-3 Ma. Lu et al. (2016b) provided an interpreted maximum depositional age of 2746+\-5 Ma for a sample of volcaniclastic mudstone. Sample GSWA 207686 (volcaniclastic metasandstone) yielded a weighted mean 207Pb/206Pb date of 2793+\-8 Ma, interpreted as a maximum age of deposition for the volcaniclastic metasandstone. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeol_lut.csv.||Unit of Poelle Group.|Includes Carlaminda Komatiite Member, Mugs Luck Basalt Member, Singleton Basalt Member.||Pyroxene-spinifex-textured basalt interlayered with thin flows of olivine spinifex-textured komatiite, interlayered with sedimentary and volcaniclastic layers in the upper part.|
77689|Yalgorup Member|69081|5|Briefly described|p737 Fig.1|Late Triassic|Late Triassic|Geol. Prov: Perth Basin.||Lesueur Sandstone.||Is overlain by Eneabba Formation; overlies Wonnerup Member (Lesueur Sandstone).||23-JUL-15
77689|Yalgorup Member|71377|5|Briefly described|p3, p7, p41-p42|Carnian|Ladinian|Perth Basin. Intersected in GSWA Harvey 1 (700-1378m). Interpreted as dominantly floodplain deposits. Formerly the Myalup Member of Crostella and Backhouse, 1999. See also p45-p47, p50-p55, p59-p64, p85, p87, p90, p102-p104.||Lesueur Sandstone||Conformably overlain by the Eneabba Formation. Overlies the Wonnerup Member.|Dark-grey coloured sandstone interbedded with subordinate finer siltstone.|
74829|Yalgowra Suite|64891|4|Described|p37 Fig. 2, p41, p44, p52-53 Tb. 1|Archean|Archean|Associated with Glen and Polelle Gps. Contains Gnanagooragoo Igneous Complex. Age: 2719+/-6Ma. Geol.prov:Murch.Dom.Mafic to ultramafic sills, ranging from dunite+ pyroxenite at base to gabbro+leucogabbro with long feathery pyroxene crystals at their tops||||||07-FEB-11
74829|Yalgowra Suite|65548|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Austin Downs Supersuite, Youanmi Terrane, Yilgarn Craton. Includes unnamed units and the Gnanagooragoo Igneous Complex.||||||
74829|Yalgowra Suite|65550|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Austin Downs Supersuite, Murchison Domain, Youanmi Terrane. Informally subdivided.||||||
74829|Yalgowra Suite|66195|4|Described|p605, 606 p598 Fig.1, p599 Fig.2|Neoarchean|Neoarchean|Yilgarn Craton. Two new ages from Pb/Pb SHRIMP zircon. Contemporaneous with komatiitic basalts of the Glen Group and granitic rocks of the Big Bell Suite.|2711 +/- 2 Ma & 2735 +/- 5 Ma.||Includes Waladah Gabbro, Fleece Pool Gabbro.|Sills emplaced into Greensleeves and Wilgie Mia Formations, Polelle Group.|Layered mafic-ultramafic sills, up to 2km thick, anhydrous and tholeiitic with a bulk composition of komatiitic basalt.|13-MAR-12
74829|Yalgowra Suite|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Mapped as seven separate but un-named units.||Unit in Austin Downs Supersuite.|||Serpentinized dunite, serpentinized peridotite, weakly metamorphosed pyroxenite, fine- to medium-grained weakly metamorphosed gabbro, coarse-grained generally massive leucogabbro, gabbro, dolerite, quartz gabbro and gabbronorite.|23-OCT-15
74829|Yalgowra Suite|67129|5|Briefly described|p18 Fig.19, p34, p36, p51-54, p60|Archean|Archean|Murchison Domain, Youanmi Terrane. Hosts some chromium, nickel, copper and PGE mineralization.|2735-2711 Ma|Austin Downs Supersuite|Waladah Gabbro.|Intrudes Greensleeves Formation. Unconformably overlain by Glen Group|Mafic-ultramafic rocks (metadunite, pyroxenite); 900m thick sill of leucogabbro with long feathery pyroxene needles.|07-SEP-17
74829|Yalgowra Suite|68108|5|Briefly described|p651 Tb.4|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane.|ca. 2735-2710 Ma; U-Pb (Ivanic et al. 2010)||||Layered gabbroic sills.|
74829|Yalgowra Suite|68110|5|Briefly described|p687|Neoarchean|Neoarchean|Murchison Domain. Appears as Yalgowra Mafic-Ultramafic Suite on p674 Fig. 2. Mainly shallow-level sills, thickness to 2 km; coeval with similar magmatism in the lower Glen Group.|<2734 - 2719 Ma.||||Komatiitic basalt.|10-OCT-14
74829|Yalgowra Suite|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane. The Yalgowra Suite consists of thick, layered mafic-ultramafic sills, most of which are emplaced into felsic volcaniclastic rocks and banded iron-formation of the Greensleeves and Wilgie Mia Formations, units which lie near the top of the Polelle Group. See also geochron file 185922.1.pdf, 185927.1.pdf.||Austin Downs Supersuite|Includes 11 unnamed units, and Fleece Pool Gabbro, Waladah Gabbro.|Intrudes Greensleeves and Wilgie Mia Formations (Polelle Group). Coeval with basalts of Glen Group, and granitic rocks of Big Bell Suite.|Dolerite; gabbro; Leucogabbro; Gabbronorite; Dunite; Peridotite; Pyroxenite; all metamorphosed or serpentinized|
74829|Yalgowra Suite|68698|5|Briefly described|p4-5, p8, p11, p17-18|Neoarchean|Neoarchean|Widespread, thick, differentiated gabbro sills; total thickness c.1km. Emplacement was coeval with deposition of Glen Group. Age range given as c.2735-2711 Ma on p11. Lu-Hf isotope data and source regions discussed.|2735 +/- 5 Ma (Wingate et al., 2010).|Austin Downs Supersuite.|Waladah Gabbro.||Gabbro sills.|
74829|Yalgowra Suite|69583|4|Described|p47, p49-50, p98, p102, p177; Plate 2|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Emplacement was coeval with deposition of, and is associated with the komatiitic basalts of, the Glen Group. About 1km thick. Brief igneous stratigraphic column.|c.2720 Ma.||Fleece Pool, Barloweerie Gabbros.|Intrudes the Greensleeves Formation.|Widespread, thick, differentiated gabbro sills; massive dolerite interleaved with minor gabbro, metamorphosed; tremolite-chlorite(-talc) schist derived from intrusive peridotite.|
74829|Yalgowra Suite|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean||||Barloweerie Gabbro, Fleece Pool Gabbro|||
74829|Yalgowra Suite|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.|||Fleece Pool, Barloweerie Gabbros.|||
74829|Yalgowra Suite|69627|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton||Austin Downs Supersuite|||Gabbro; massive to weakly foliated; local dolerite, quartz gabbro and gabbronorite; weakly metamorphosed.|
74829|Yalgowra Suite|70020|4|Described|p113,117-118,120,130|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton. Cumulative thickness: ~1km. Emplacement of widespread, thick and differentiated mafic-ultramafic sills in shallow crust is coeval with deposition of Wattagee Formation, and drove hydrothermal circulation. Age is constrained by U-Pb dates of 2735+\-5 Ma, 2719+\-6 Ma, and 2711 +\-2 Ma (Ivanic et al., 2010).|||Includes Fleece Pool gabbro, Kathleen Valley gabbro, Dalgaranga dolerite and Waladah gabbro.|Underlain by Boodanoo Suite.|Komatiitic basalt.|
74829|Yalgowra Suite|70139|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton. The two facies are mapped separately.|c.2735 Ma.|Austin Downs Supersuite.|||Peridotite, fine- to medium-grained, serpentinized and locally foliated; gabbro, massive to weakly foliated, local dolerite, quartz gabbro, gabbronorite: weakly metamorphosed.|
74829|Yalgowra Suite|70418|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. The two facies associations are separately mapped.|2735-2711 Ma.|Austin Downs Supersuite.|||Fine- to medium-grained peridotite, serpentinised and locally foliated. Massive to weakly foliated gabbro, local dolerite, quartz gabbro, and gabbronorite, weakly metamorphosed.|
74829|Yalgowra Suite|70419|5|Briefly described|p2, p8, p12|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Mafic-ultramafic intrusives. Density is 3.06 g/cm3.|c.2.72 Ga.||Barloweerie gabbro.|||
74829|Yalgowra Suite|70796|4|Described|100k_geologyl_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 185922.1.pdf, Austin100_2442_stratig.pdf, Cue100_2443_stratig.pdf, Madoonga100_2444_stratig.pdf, MountMagnet100_2441_stratig.pdf, Reedy100_2543_stratig.pdf, Tieraco100_2545_stratig.pdf. Numerous additional lithologies are discussed.|ca 27352711 (inferred)|Austin Downs Supersuite|Includes the Fleece Pool Gabbro and the Waladah Gabbro.|Intrudes the Greensleeves and Wilgie Mia formations. Coeval with the Glen Group and the Big Bell Suite.|Gabbro; massive to weakly foliated; local dolerite, quartz gabbro, and gabbronorite; weakly metamorphosed. Peridotite, fine to medium grained; serpentinized and locally foliated. Schist, leucogabbro and dunite are also present.|
74829|Yalgowra Suite|70830|4|Described|p2, p4-p5, p7, p9, p11|Neoarchean|Neoarchean|Youanmi Terrane. The cumulative thickness of the sills of this suite is 1.5km. See also p13-p14, p27-p28, p51, p53.|c. 2720 Ma|Austin Downs Supersuite||Intrudes the Greensleeves Formation (Polelle Group).|Mafic and ultramafic rocks.|
74829|Yalgowra Suite|71148|6|Mentioned|p120, 122|Neoarchean|Neoarchean|Cue Zone, NE Youanmi Terrane, Yilgarn Craton.|c.2725 Ma.||||Mafic magmatics.|
74829|Yalgowra Suite|71168|4|Described|p7-p8, p10|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. See also p19 fig 11, p24-p25, p60-61.|C. 2730 Ma||Includes the Dalgaranga dolerite, Waladah Gabbro, Fleece Pool Gabbro.|Intrudes the Greensleeves Formation.|Komatiitic basalt. Mafic-ultramafic sills.|
74829|Yalgowra Suite|71269|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Sills and dykes have been dated ar 2719+\-6 Ma and 2711+\-2 Ma (Pidgeon and Hallberg, 2000; Wingate et al., 2010). Sample GSWA 185922 (mafic sill) yielded a weighted mean 207Pb/206Pb date of 2735+\-5 Ma, interpreted to be igneous crystallisation age. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeol_lut.csv.|2735-2711 Ma|Unit of Austin Downs Supersuite.|Includes Fleece Pool Gabbro, Opal Gabbro, Waladah Gabbro.|Intrudes into Greensleeves and Wilgie Mia formations. Coeval with Glen Group and Big Bell Suite.|Dolerite interleaved with minor gabbro and weakly foliated granitic rock; metamorphosed, gabbro and leucogabbro, quartz gabbro, gabbronorite, melanocratic and leucocratic gabbro, dunite, peridotite, pyroxenite.|
74829|Yalgowra Suite|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.||Austin Downs Supersuite.|Waladah, Opal Gabbros.||Layered mafic-ultramafic intrusive rocks: dominantly gabbro; minor basal ultramafic rocks; weakly metamorphosed, variably deformed. Five facies are mapped separately.|
74829|Yalgowra Suite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Youanmi Terrane.|||||Massive dolerite interleaved with minor gabbro; metamorphosed.|
74829|Yalgowra Suite|73023|5|Briefly described|p15|Neoarchaean|Neoarchaean|Emplacement is consistent with lithospheric extension and onset of a mantle plume event across the Yilgarn Craton.|2735-2711 Ma.||||Gabbroic sills with pyroxenite to peridotite cumulate bases.|
74829|Yalgowra Suite|73596|6|Mentioned|p1160, 1165, 1169|Neoarchean|Neoarchean|Youanmi Terrane. Within the upper Glen Group stratigraphy.|2735-2710 Ma.|Glen Group.|Fleece Pool, Waladah Gabbros; Dalgaranga Dolerite.||Gabbro sills.|
31767|Yallalong Granite|23569|4|Described|p5 Tb. 1|Archean|Archean|Of the Narryer Terrane.   Coarse-grained, equigranular, leucocratic granulite-facies monzogranite.||||||07-NOV-08
31767|Yallalong Granite|23574|5|Briefly described|Map Legend|Archean|Archean|Underlying unit Wandarrie Granite||||||07-NOV-08
31767|Yallalong Granite|23576|5|Briefly described|Map Legend|Archean|Archean|Underlying unit Wandarrie Granite||||||07-NOV-08
31767|Yallalong Granite|23577|5|Briefly described|Map Legend|Archean|Archean|Underlying unit Wandarrie Granite.||||||07-NOV-08
31767|Yallalong Granite|24114|5|Briefly described|p5 Fig.4|Archean|Archean|Geological Province: Yilgarn Craton. Age: c. 2685 Ma||||||07-NOV-08
31767|Yallalong Granite|43835|5|Briefly described|Map Legend|Archean|Archean|Age about 2685Ma.||||||07-NOV-08
31767|Yallalong Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzonite|
31767|Yallalong Granite|73526|5|Briefly described|p2 Fig.1, p3|Neoarchean|Neoarchean|Narryer Terrane, western. See also Yallalong granite p4 Tb.1, age of 2683+/-4 Ma.|c. 2685 Ma||||Heterogeneous, complexly deformed quartzofeldspathic gneiss containing amphibolite enclaves.|
41172|Yallingarrintha Tonalite|50370|5|Briefly described|Map Legend|Archean|Archean|Of Yule Granitoid Complex. Geological Province: Pilbara Craton||||||07-NOV-08
41172|Yallingarrintha Tonalite|50379|5|Briefly described|Map Legend|Archean|Archean|Of Yule Granitoid Complex. Geological Province: Pilbara Craton. Age: c. 3420 Ma||||||07-NOV-08
41172|Yallingarrintha Tonalite|63372|4|Described|Map Legend|Archean|Archean|Of the Yule Granitoid Complex. Age: 3420 Ma. Geological Province: East Pilbara Granite-Greenstone Terrane. Biotite-hornblende bearing tonalite; moderatly to strongly foliated; metamorphosed||||||15-APR-13
41172|Yallingarrintha Tonalite|63441|5|Briefly described|p7 Tb. 2|Archean|Archean|Of the Tambina Supersuite. Age: 3421 +/-2 Ma. Geological province: Pilbara Craton.||||||15-APR-13
41172|Yallingarrintha Tonalite|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Tambina Supersuite. Age shown as c. 3421 Ma. Meta biotite-hornblende tonalite to metagranodiorite; moderately to strongly foliated.||||||15-APR-13
41172|Yallingarrintha Tonalite|69013|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane.|c. 3421 Ma|Of the Tambina Supersuite.|||Comprises meta biotite-hornblende tonalite to metagranodiorite; moderately to strongly foliated.|29-APR-14
41172|Yallingarrintha Tonalite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Tambina Supersuite|||Meta biotite--hornblende tonalite and metagranodiorite; moderately to strongly foliated|
41172|Yallingarrintha Tonalite|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|3421 Ma (isotopic)|Unit of Tambina Supersuite.|||Metamorphosed biotite-hornblende tonalite and metagranodiorite; moderately to strongly foliated|
41172|Yallingarrintha Tonalite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||tonalite, granodiorite|
74899|Yallum Hill Member|64655|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Glenayle Dolerite. Medium- to coarse-grained dolerite, locally mesocratic and granophyric; in places layered with gabbroic base; local superposition of sills indicated by l (lower) and u (upper).||||||27-NOV-08
74899|Yallum Hill Member|64772|5|Briefly described|p13|Mesoproterozoic|Mesoproterozoic|Of the Glenayle Dolerite.||||||07-FEB-11
74803|Yaloginda Formation|64891|4|Described|p37 Fig. 2, p38, p48-9 Tb. 1|Archean|Archean|Of the Norie Group. Conformable on Murrouli Basalt. Max. age: 2815-2800Ma. Geological province: Murchison Domain. Consists of fine- to medium-grained felsic volcaniclastic sedimentary rocks and interbedded BIF, local quartzite.||||||07-FEB-11
74803|Yaloginda Formation|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|2815 - 2800 Ma.|Unit in Norie Group.|||Felsic volcaniclastic rocks and banded iron-formation; local quartzite; widely intruded by layered gabbroic to peridotite sills; metamorphosed (section only).|
74803|Yaloginda Formation|67129|6|Mentioned|p18 fig 19|Archean|Archean|Murchison Domain, Youanmi Terrane.||Norie Group|Includes Kantie Murdana Volcanics Member|||07-SEP-17
74803|Yaloginda Formation|68110|4|Described|p673, p674 Fig.2|Neoarchean|Mesoarchean|Murchison Domain.|c. 2815-2792 Ma|Of the Norie Group.||Overlies Murrouli Basalt. Intruded and overlain by the Polelle Group.|Felsic volcaniclastic and volcanic rocks, banded iron formation, quartzite.|
74803|Yaloginda Formation|68287|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean||~ 2813-2820 Ma|Of the Norie Group|Includes Kantie Murdana Volcanics Member and 5 other unnamed units.||Metarhyolitic and serpentinitic lenses; felsic schist; psammitic to pelitic schist, locally strongly sheared; strongly foliated metachert, locally ferruginous; metabanded iron-formation typically with recrystallized magnetite crystals.|
74803|Yaloginda Formation|68519|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|2815-2800 Ma|Unit in Norie Group.|Includes Kantie Murdana Volcanics Member.||Metasiliciclastic rocks: psammitic schist, felsic schist, strongly foliated metachert, meta banded iron-formation.|
74803|Yaloginda Formation|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane. Thickness ~500m. Age: magmatic crystallization age of the rhyolite. From Geochron file 178142.1.pdf. See also 183953.1.pdf, 185998.1.pdf.|2806+/-4Ma Pb/Pb SHRIMP|Norie Group|Includes Kantie Murdana Volcanics Member and 20 unnamed subunits.||Fine- to medium-grained felsic volcaniclastic and volcanic rocks, and interbedded units of ferruginous shale and/or banded iron-formation; local quartzite; widely intruded by layered gabbroic to peridotite sills; metamorphosed|23-OCT-15
74803|Yaloginda Formation|68698|5|Briefly described|p4, p7, p11|Mesoarchean|Mesoarchean|Igneous crystallisation age (Wingate et al., 2011).|2814 +/- 3 Ma to 2806 +/- 4 Ma.|Norie Group.||Conformably overlies Murrouli Basalt. Is overlain by Coodardy Formation (Polelle Group).|Rhyolite, fine- to medium-grained felsic volcaniclastic sedimentary rocks, and interbedded units of ferruginous shale and/or BIF.|
74803|Yaloginda Formation|69014|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane. 7 facies are mapped separately.|2815-2805 Ma|Of the Norie Group.|Includes the Kantie Murdanna Volcanics Member.||Undivided: felsic volcaniclastic rocks and banded iron-formation; local quartzite; widely intruded by layered gabbroic to peridotitic sills; metamorphosed.|01-MAY-14
74803|Yaloginda Formation|69583|4|Described|p47, p49, p97, p108, p153; Plate 2|Mesoarchean|Mesoarchean|Murchison Domain, western Youanmi Terrane. Geochronology by Van Kranendonk and Ivanic (2009). Seismic interpretation.|2814 +/- 3 Ma to 2806 +/- 4 Ma.|Norie Group.|Kantie Murdana Volcanics Member.|Conformably overlies Murrouli Basalt.|Rhyolite, fine- to medium-grained felsic volcaniclastic sedimentary rocks (felsic schists), and interbedded units of ferruginous shale and BIF.|
74803|Yaloginda Formation|69584|5|Briefly described|p2, p5 Fig.2, p6, p59|Mesoarchean|Mesoarchean|Youanmi Terrane, Yilgarn Craton. Meekatharra area. Contains the Austin VMS deposit of copper, zinc, silver and gold. Mineralization is associated with talc and amphiboles.||Norie Group|Kantie Murdanna Volcanics Member, Yuinmery Volcanics Member|Overlies the Murrouli Basalt.|Felsic volcaniclastic rocks, iron rich sediments and banded iron formations.|28-AUG-20
74803|Yaloginda Formation|69586|5|Briefly described|p22, p31 Fig.33|Neoarchean|Neoarchean|Murchison Domain.||Norie Group.|Kantie Murdanna Volcanics Member.|||
74803|Yaloginda Formation|69626|5|Briefly described|map legend|Archean|Archean|Detailed lithology in legend. Murchison Domain, Youanmi Terrane, Yilgarn Craton||Norie Group|||Psammitic/granitic/pelitic schist; metasiliciclastics(psammite, pelite); quartzite; metamorphosed andesitic, dacitic, felsic volcanics/volcaniclastics; BIF; chert; volcanic conglomerate/sandstone; rhyolitic to rhyodacitic breccia/tuff, rhyolitic lava|
74803|Yaloginda Formation|69627|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Detailed lithology in legend. |2815-2805 Ma|Norie Group|||Felsic volcaniclastic rocks and banded iron-formation; local quartzite; widely intruded by layered gabbroic to peridotitic sills; metamorphosed.|
74803|Yaloginda Formation|69628|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Detailed lithology in legend. |2815-2805 Ma|Norie Group|||Rhyolite and rhyolitic volcaniclastic rocks; fine- to medium-grained; massive to crudely bedded; metamorphosed.|
74803|Yaloginda Formation|69744|6|Mentioned|p259|||Mount Magnet Greenstone Belt.|~2800 Ma.||||Metabasalts and BIF.|
74803|Yaloginda Formation|70020|5|Briefly described|p117-118,123,126,128-129|Mesoarchean|Mesoarchean|Geological province: Murchison Domain, Yilgarn Craton. Thickness: c. 500m thick. Contains felsic rocks associated with VHMS mineralization and are display prospective geochemical characteristics. Characterized by tholeiitic to transitional felsic rocks with flat RE Eprofiles and HFSE enrichment (Van Kranendonk et al., 2013).||Unit of Norie Group.||Overlain disconformably by Coodardy/Mougooderra Formation/Polelle Group. Underlain by Murrouli Basalt.||
74803|Yaloginda Formation|70030|5|Briefly described|p192|Mesoarchean|Mesoarchean|Geological province: Murchison Domain, Yilgarn Craton.||Unit of Norie Group.|Includes K-M Volcanics.|Upper unit of Norie Group. Overlain by Coodardy Formation/Polelle Group. Underlain by Murrouli Basalt.||
74803|Yaloginda Formation|70139|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Seven facies are mapped separately.||Norie Group.|||Metamorphosed rhyolite, rhyolitic volcaniclastic rock, banded iron-formation, ferruginous banded chert, foliated metabasalt and local amphibolite, metabasalt and metakomatiitic basalt, felsic schist after volcanic rock, local quartzite.|
74803|Yaloginda Formation|70140|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. The 7 facies are mapped separately.||Norie Group.|Youangarra and Yuinmery, Volcanics Members.||Psammite; psammitic schist; felsic schists: all strongly sheared. Porphyritic dacite and rhyolite lavas; foliated BIF: all metamorphosed.|
74803|Yaloginda Formation|70418|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Five facies are mapped separately.||Norie Group.|||Felsic volcaniclastic rocks and BIF; local quartzite; widely intruded by layered gabbroic to peridotitic sills; metamorphosed.|
74803|Yaloginda Formation|70419|5|Briefly described|p1-2, p15|||||Norie Group.|Kantie Murdana Volcanics Member.||Felsic schists.|
74803|Yaloginda Formation|70770|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Six facies are mapped separately.|2825-2800 Ma.|Norie Group.|||Banded BIF and ferruginous banded chert; andesitic and dacitic volcanic and volcaniclastic rock; both metamorphosed. Quartzite; psammitic schist locally grading into pelitic schist; pelite, locally strongly sheared; metasiliciclastic rocks.|
74803|Yaloginda Formation|70796|4|Described|100k_geologyl_lut.csv|Neoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_geologysub_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 178142.1.pdf, 183953.1.pdf, 185998.1.pdf, 198209.1.pdf, 198210.1.pdf, Austin100_2442_stratig.pdf, Bungar100_2539_stratig.pdf, Challa100_2541_stratig.pdf, Coolamaninu100_2540_stratig.pdf, MountMagnet100_2441_stratig.pdf, Nowthanna100_2643_stratig.pdf, Reedy100_2543_stratig.pdf, Windimurra100_2641_stratig.pdf, Wynyangoo100_2542_stratig.pdf, Youanmi100_2640_stratig.pdf. Numerous additional lithologies are discussed. 500m thick.|ca 2815 to 2800 Ma (inferred)|Norie Group|Includes the Kantie Murdana Volcanics Member, Yuinmery Volcanics Member and the Youangarra Volcanics Member.|Overlies the Murrouli Basalt. Overlain by the Polelle Group.|Felsic volcaniclastic rocks and banded ironformation; local quartzite and felsic schist; Metasiliciclastic rocks; Psammitic and pelitic schist; quartzite; strongly foliated metachert.|
74803|Yaloginda Formation|70830|5|Briefly described|p7, p9|||||Norie Group||Conformably overlies the Murrouli Basalt.|Rhyolite, fine- to medium-grained felsic volcaniclastic sedimentary rocks with interbedded ferruginous shale and banded iron formation.|
74803|Yaloginda Formation|71159|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton. The three facies are mapped separately.||Norie Group.|Kantie Murdana Volcanic Member.||Felsic schist, locally strongly sheared; metamorphosed BIF, foliated; psammitic schist, locally grading into pelitic schist or quartzite, locally strongly sheared, contains metasedimentary xenoliths.|
74803|Yaloginda Formation|71168|4|Described|p7-p8, p18-p19|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Approximately 500m thick. Associated with VMS mineralization. Petrochemically prospective. This unit is interpreted to be the extrusive equivalent of the Mount Kenneth Suite. See also p43, p51, p56, p59.|c. 2815 Ma|Norie Group|Includes the Kantie Murdana Volcanics Member.|Conformably overlies the Murrouli Basalt. Overlain by the Coodardy and Mougooderra Formations (Polelle Group).|Felsic volcaniclastic and volcanic rocks that are interbedded with ferruginouys shale and/or banded iron formation.|
74803|Yaloginda Formation|71269|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Approximately 500m thick. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). Previously geochronological results include 2817+\-3 Ma and 2814+\-2 Ma (Wingate et al., 2011a,b), interpreted to be maximum depositional age. Sample GSWA 178142 (metamorphosed, flow-banded rhyolite) yielded a weighted mean 207Pb/206Pb date of 2806+\-4 Ma, interpreted to be magmatic crystallisation age of rhyolite. Sample GSWA 183953 (felsic volcaniclastic) yielded a weighted mean 207Pb/206Pb date of 2814+\-2 Ma, interpreted to be maximum depositional age. Sample GSWA 185998 (qtz ch-ms schist) yielded a weighted mean 207Pb/206Pb date of 2817+\-3 Ma, interpreted to be maximum depositional age. Sample GSWA 198209 (felsic schist) yielded a weighted mean 207Pb/206Pb date of 2813+\-5 Ma, interpreted to be magmatic crystallization age of the felsic volcanic protolith of the schist. Sample GSWA 205750 (felsic metavolcanic rock) yielded a weighted mean 207Pb/206Pb date of 2810+\-4 Ma, interpreted to be magmatic crystallization age of the rock. See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeol_lut.csv, 100k_geologysub_lut.csv.|2815-2800 Ma|Unit of Norie Group.|Includes Kantie Murdana Volcanics Member, Youangarra Volcanics Member.|Overlain by Coodardy Formation. Underlain by Murrouli Basalt.|Felsic volcaniclastics, BIFs, local quartzite and felsic schist, psammitic and pelitic schist, granitic schist, metabasalt and metakomatiitic basalt, quartzite, rhyolite and rhyolitic to rhyodacitic volcaniclastics, breccias and tuffs.|
74803|Yaloginda Formation|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|2815-2800 Ma.|Norie Group.|||Felsic volcanic and volcaniclastic rock; BIF, jaspilite, chert, shale, associated mafic rock; BIF and ferruginous banded chert; BIF with coarse granular and recrystallised magnetite crystals; siliciclastic rocks. All metamorphosed.|
74803|Yaloginda Formation|71311|5|Briefly described|p795, p799, p802-804|||Mount Magnet greenstone belt area. Deformation described.|2.80 Ga.||||Greenstones. Metabasalts, metamorphosed BIF and chert.|
74803|Yaloginda Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Youanmi Terrane. ||Norie Group|Includes Kantie Murdana Volcanics Member and an unnamed subunit.||Felsic volcaniclastic rocks + banded iron-formation; local quartzite and felsic schist; widely intruded by layered gabbroic to peridotitic sills; metamorphosed. Banded iron-formation, jaspilite, chert, shale w associated mafic rock; metamorphosed.|
74803|Yaloginda Formation|72389|5|Briefly described|Map Legend|Archean|Archean|Gabanintha 1:100k map sheet 2644. Includes numerous unnamed constituents.||Norie Group|||Felsic volcaniclastic rocks and banded iron-formation; locally quartzite and felsic schist; widely intruded by layered gabbroic to peridotitic sills; metamorphosed.|
74803|Yaloginda Formation|72494|5|Briefly described|p15-16, 18, 22|||Youanmi Terrane, Yilgarn Craton. Geochemistry plots.|~2815 - 2806 Ma.|||Overlies Singleton Formation.|Felsic volcanic and volcaniclastic rocks and BIF; local intercalated quartzite and BIF at the top of the unit.|
74803|Yaloginda Formation|73410|6|Mentioned|p13|||||Norie Group.||||
74803|Yaloginda Formation|73596|6|Mentioned|p1170|Neoarchean|Mesoarchean|Youanmi Terrane, Yilgarn Craton. Several geochronology determinations given.|2815 +/- 7 Ma to 2798 +/- 8 Ma.|Norie Group.||||
30815|Yamagee Granite|23485|5|Briefly described|p20|||Of Bertibubba suite.||||||
30815|Yamagee Granite|50218|5|Briefly described|p249|Orosirian|Orosirian|Of the Bertibubba Supersuite. Age: ca.1960Ma.||||||07-FEB-11
30815|Yamagee Granite|65549|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Bertibubba Supersuite, Gascoyne Province. Age of c. 1960 Ma given.||||||
30815|Yamagee Granite|65896|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gascoyne Complex. c.1960 Ma. Foliated, medium- to fine-grained, even-textured, biotite monzogranite; minor leucocratic biotite-garnet monzogranite.||||||
30815|Yamagee Granite|66299|5|Briefly described|pp106-107, p187.|Paleoproterozoic|Paleoproterozoic||1958 +/- 4 Ma.|Unit in Bertibubba Supersuite.||Intrudes Yarlarweelor Gneiss Complex. Is intruded by sheets, dykes and veins of Moorarie Supersuite.|Foliated, medium- and fine-grained, equigranular biotite metamonzogranite; minor leucocratic biotite-garnet metamonzogranite.|
30815|Yamagee Granite|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|||Bertibubba Supersuite|||Foliated, medium- and fine-grained, equigranular biotite metamonzogranite, porphyritic biotite metamonzogranite; minor leucocratic biotite-garnet metamonzogranite|
30815|Yamagee Granite|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_interpgeop_lut.csv|1958 Ma||||Foliated, medium and fine grained, equigranular biotite metamonzogranite; minor leucocratic biotite-garnet metamonzogranite. Medium grained, porphyritic biotite metamonzogranite; round phenocrysts of K-feldspar; foliated.|
27027|Yampi Formation|23722|4|Described|p21|Paleoproterozoic|Paleoproterozoic|Formerly Yampi Member of Pentecost Sandstone.   Parent: Kimberley Group.   Geological Province: Kimberley Basin||||||07-NOV-08
27027|Yampi Formation|42814|4|Described|p15|||Formerly Yampi Member of Pentecost Sandstone. Now of Kimberley Group.||||||
27027|Yampi Formation|42815|5|Briefly described|map|Proterozoic||||||||
27027|Yampi Formation|43281|5|Briefly described|Map legend||Proterozoic|Of Kimberley Group.||||||09-DEC-08
27027|Yampi Formation|64580|4|Described|map legend||Paleoproterozoic|Of Kimberley Group. Feldspathic and hematitic sandstone; minor siltstone.||||||09-DEC-08
27027|Yampi Formation|68078|6|Mentioned|p6, p21 figure 14, p23|Paleoproterozoic|Paleoproterozoic|Only present at the northwestern end of the halls creek orogen. ||Kimberley Group||Overlies Pentecost Sandstone||13-SEP-22
27027|Yampi Formation|69003|6|Mentioned|p21|Paleoproterozoic|Paleoproterozoic|||||Overlies Pentecost Sandstone.||
27027|Yampi Formation|69099|5|Briefly described|500k_geologyp08_lut.csv||Paleoproterozoic|||Of Kimberley Group in 2008.|||Feldspathic and hematitic sandstone; minor siltstone.|04-AUG-15
27027|Yampi Formation|69585|6|Mentioned|p4-5, p22|Statherian|Statherian|Western Lamboo Province. May be correlative with an informal upper member of Pentecost Sandstone.||Kimberley Group.||||
27027|Yampi Formation|69634|5|Briefly described|500k_geologyp08_lut.csv||Paleoproterozoic|||Unit of Kimberley Group.|||Feldspathic and hematitic sandstone; minor siltstone|
27027|Yampi Formation|70154|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic||1740-1835 Ma|Kimberley Group|||Pink-brown arkose and feldspathic sandstone; minor siltstone, hematitic quartz sandstone, glauconitic sandstone|
27027|Yampi Formation|70812|5|Briefly described|p6|Statherian|Statherian|Western Zone of the Halls Creek Orogen, Lamboo Province.|c. 1750 Ma|||||
27027|Yampi Formation|70851|5|Briefly described|p4|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province.|c. 1750 Ma|||||
27027|Yampi Formation|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|1835-1740 Ma (inferred)|Unit of Kimberley Group.|||Proximal-littoral pink-brown arkose and feldspathic sandstone, minor siltstone, haematitic quartz sandstone, glauconitic sandstone, and quartz pebble conglomerate|
27027|Yampi Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Kimberley Basin.||Kimberley Group, upper|||Pink-brown arkose and feldspathic sandstone; minor siltstone, hematitic quartz sandstone, glauconitic sandstone.|
24134|Yandagooge Formation|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Rudall Complex, Paterson Orogen.||||||
24134|Yandagooge Formation|23590|5|Briefly described|p8|||Previously called Yandagooge Inlier. Geological Province: Fingoon Domain.||||||
24134|Yandagooge Formation|23602|4|Described|p11|||See also page 6 Table 1. Of Rudall Complex. Max. thickness: 1500 m.||||||
24134|Yandagooge Formation|23760|4|Described|p15|Paleoproterozoic|Paleoproterozoic|Geological Province: Talbot Terrane. Max. thickness: 1500 m.||||||07-NOV-08
24134|Yandagooge Formation|42278|4|Described|p35|||See also Fig.3||||||
24134|Yandagooge Formation|42702|5|Briefly described|map legend|Proterozoic||||||||
24134|Yandagooge Formation|43118|5|Briefly described|Table 1,p13|||of Rudall Complex||||||
24134|Yandagooge Formation|43348|4|Described|P8, p5, table 1 p6,7|Mesoproterozoic|Paleoproterozoic|Of Rudall Complex||||||07-NOV-08
24134|Yandagooge Formation|43697|6|Mentioned|p25|||Older part of the Rudall Complex. Banded orthogneiss and metasediments.  Occurs as inclusions in, and is intimately interlayered with, a composite orthogneiss that is the dominant rock type of the complex.||||||08-AUG-05
24134|Yandagooge Formation|43847|5|Briefly described|Map Legend||Proterozoic|||||||
24134|Yandagooge Formation|43848|5|Briefly described|Map Legend||Proterozoic|||||||
24134|Yandagooge Formation|50436|5|Briefly described|p2.1|||Conformably overlies: Fingoon Quartzite. Underlies: Butler Creek Formation, Poynton Formation. Includes: Cassandra Member. Intruded by: Kalkan Supersuite.||||||09-AUG-04
24134|Yandagooge Formation|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Pelitic to semi-pelitic quartz-mica schist and hematite-biotite schist; minor quartzite, felsic gneiss, pyritic graphitic schist, chert, and metamorphosed banded iron-formation.||||||09-DEC-08
24134|Yandagooge Formation|64943|4|Described|p11, p4-6, 8-9, 10,19-21,28, 2,35,38-39|Statherian|Statherian|Talbot Terrane, Rudall Complex. <1500m thick. Quartz-muscovite schist. Underlies Butler Creek Fm. Includes Cassandra Member. Transitionally overlies Fingoon Quartzite. Intruded by granitoids 1787-1765 Ma (zircon U-Pb, Nelson 1995); type locality given.||||||09-MAY-16
24134|Yandagooge Formation|65404|6|Mentioned|p247|||A division of the Talbot terrane by Clarke (1991). Preserves low-pressure metamorphism at amphibolite facies.||||||
24134|Yandagooge Formation|65454|4|Described|p4, p7 Fig.3, p13, p30 Fig.A1b|Statherian|Statherian|Of Fingoon Package, Talbot Terrane. Predominantly pelitic to semi-pelitic assemblage of quartz-muscovite schist, hematitic biotite schist, and minor intercalations of muscovite quartzite with minor psammitic gneiss, graphitic schist, chert, and banded iron formation. Hosts many uranium and base metal prospects in the Talbot Terrane.|Inferred to be older than 1680+/-29 Ma metamorphic|||||21-APR-16
24134|Yandagooge Formation|67182|5|Briefly described|p677 Fig.2, p678|Mesoproterozoic|Paleoproterozoic|Paterson Orogen. Hosts the Kintyre uranium deposit. Calculated chemical (U-Th-Pb, EPMA analyses) ages for uraninite in the Kintyre deposit range 773 to 912 +/- 35 Ma, with a median of 837 +/- 31-35 Ma which is best interpreted as reconnaissance-level age determination. This age is in good agreement with the ca 845 Ma estimate for the deposit (Maas unpublished, cited Huston et al. 2009).  ||||Unconformably underlies Coolbro Sandstone|Carbonaceous metasediments.|
24134|Yandagooge Formation|67202|4|Described|p5, p56, p121, p150, p156, p161-163|Paleoproterozoic|Paleoproterozoic|See also p179, p222, p233, p235, p238-243, p247, p272, p277, p279-281. Talbot Terrane, Rudall Complex. Less than 1500m thick. Hosts polymetallic U mineralisation in pitchblende veins at Kintyre (deposit described in detail). Conductivity discussed briefly. Minimum age from intruding granite.|>1790 Ma.|Rudall Complex.|||Complexly folded and faulted greenschist facies retrograde metamorphic rocks: quartz-muscovite schist, meta-pelitic rocks, BIF, chert, graphitic schist and biotite schist.|
24134|Yandagooge Formation|67430|5|Briefly described|p21-22|Mesoproterozoic|Paleoproterozoic|Paterson Orogen. Hosts the unconformity-related Kintyre U deposit in chlorite-carbonate veins; dated at ~840-830 Ma.||||Is overlain unconformably by Coolbro Sandstone.|Carbonaceous metasediments.|
24134|Yandagooge Formation|68981|5|Briefly described|p2-3|||Eastern Talbot Terrane, Rudall Province.||||Conformably overlies Fingoon Quartzite. Is overlain by the Butler Creek and Poynton Formations.|Quartz-muscovite schist, iron-rich graphitic pelitic schist, banded iron-formation, and chert.|
24134|Yandagooge Formation|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|Talbot and Connaughton Terranes (Rudall Province).||||||
24134|Yandagooge Formation|71169|5|Briefly described|p3-p4, p6-p7|||See also  p14-p15, p18, p25, p60, p70.||||Structurally overlies the Fingoon Quartzite. Structurally overlain by the Butler Creek Formation.|Pelitic and psammitic metasedimentary rocks and banded-iron formation, chert and iron-rich graphitic rocks.|
24134|Yandagooge Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, psammite, schist, pelite|
24134|Yandagooge Formation|71795|6|Mentioned|p35 fig 4|||Rudall Province.||||||
24134|Yandagooge Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Talbot Zone, Rudall Province, Paterson Orogen.|||||Pelitic to semi-pelitic quartz--mica schist and hematite--biotite schist; minor quartzite, felsic gneiss, pyritic graphitic schist, chert, and metamorphosed banded iron-formation.|
24134|Yandagooge Formation|73168|6|Mentioned|p741 Fig.2|Mesoproterozoic|Paleoproterozoic|Rudall Province.||||||
38646|Yandal Sandstone|23786|5|Briefly described|p5|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
38646|Yandal Sandstone|60623|5|Briefly described|p33|Archean|Archean|Fluvial unit equivalent to Merougil Formation.||||||07-NOV-08
38646|Yandal Sandstone|64633|6|Mentioned|p6 Fig.4.|||?Kalgoorlie Terrane or later basin.|<2680 +/- 6 Ma.|||||24-APR-17
38646|Yandal Sandstone|66880|6|Mentioned|p8 Fig.2. |Archean|Archean|Kalgoorlie Terrane.|2680 +/- 6 Ma.|||||
26240|Yandanooka Group|22716|5|Briefly described|table4, p238|Tonian|Stenian|Age: 1000 Ma. Equivalent to Moora Group of the Yilgarn Craton.||||||
26240|Yandanooka Group|23172|4|Described|Map Legend|Proterozoic|Proterozoic|||||||
26240|Yandanooka Group|23174|6|Mentioned|p9||Proterozoic|||||||
26240|Yandanooka Group|23279|5|Briefly described|p10||Proterozoic|||||||
26240|Yandanooka Group|23761|6|Mentioned|p4 Fig. 2|Proterozoic|Proterozoic|Mainly well-cemented and indurated sandstone and siltstone.   Max. thickness: >5000m.   Geological Province: Yilgarn Block.  See also p12.||||||
26240|Yandanooka Group|23762|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
26240|Yandanooka Group|23788|5|Briefly described|p5|Proterozoic|Proterozoic|Geological Province: Yilgarn Craton.||||||
26240|Yandanooka Group|23816|5|Briefly described|p229|Proterozoic|Proterozoic|Max. thickness: >10 000 m.||||||20-NOV-09
26240|Yandanooka Group|24058|5|Briefly described|p111|Precambrian|Precambrian|||||||20-NOV-09
26240|Yandanooka Group|24160|6|Mentioned|p23|||||||||
26240|Yandanooka Group|24410|5|Briefly described|p141 Fig. 82|||||||||24-NOV-09
26240|Yandanooka Group|24526|5|Briefly described|p106 Fig. 7|Neoproterozoic|Neoproterozoic|Of the Mullingarra Complex. Comprises undeformed but steeply dipping siltstone, conglomerate and sandstone.  Geological Province: Perth Basin.||||||02-MAR-05
26240|Yandanooka Group|24542|5|Briefly described|p2 Fig.2, p11|Proterozoic|Proterozoic|Unconformably overlies Mullingarra Complex. Siltstone, conglomerate and sandstone.||||||16-JAN-07
26240|Yandanooka Group|31154|6|Mentioned|p71|||||||||
26240|Yandanooka Group|31393|6|Mentioned|Pl.25|||||||||
26240|Yandanooka Group|31910|6|Mentioned|p16|||||||||
26240|Yandanooka Group|33044|6|Mentioned|p32|||||||||
26240|Yandanooka Group|33625|6|Mentioned|p198|||||||||
26240|Yandanooka Group|34274|6|Mentioned|p116|||?Prot. Fig.1||||||
26240|Yandanooka Group|35282|6|Mentioned|p9|||||||||
26240|Yandanooka Group|36293|2|Defined|p52|Neoproterozoic|Mesoproterozoic|Middle or Late Proterozoic.||||||
26240|Yandanooka Group|36551|6|Mentioned|p141|||||||||
26240|Yandanooka Group|36872|4|Described|p72|||Formerly Yandanooka Beds||||||
26240|Yandanooka Group|36879|6|Mentioned|p106|||||||||
26240|Yandanooka Group|37298|6|Mentioned|Fig.1|||||||||
26240|Yandanooka Group|37344|6|Mentioned|p74|||||||||
26240|Yandanooka Group|37460|4|Described|p177|||||||||
26240|Yandanooka Group|37915|6|Mentioned|p461|||||||||
26240|Yandanooka Group|38769|6|Mentioned|p79|||||||||
26240|Yandanooka Group|40089|6|Mentioned|p12|||||||||
26240|Yandanooka Group|40307|6|Mentioned|p62|||||||||
26240|Yandanooka Group|40346|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26240|Yandanooka Group|40347|4|Described|p15|||||||||
26240|Yandanooka Group|41271|6|Mentioned|p228|||||||||
26240|Yandanooka Group|41341|6|Mentioned|p8|||||||||
26240|Yandanooka Group|43096|6|Mentioned|p3|||||||||
26240|Yandanooka Group|43442|5|Briefly described|p43,47||Proterozoic|Part of Pinjara Orogen, not Perth Basin||||||
26240|Yandanooka Group|43495|6|Mentioned|5|||||||||
26240|Yandanooka Group|44138|4|Described|p264 Fig.3-54, p265, p272|||5m thick [ possibly 5km?]. Very low grade metamorphism, but dips steeply.||||Possibly correlated to Billeranga Subgroup of Moora Group. Overlies Mullingarra Complex (unconformably).|Well-laminated or massive siltstone, wacke and turbidite with volcanic detritus; basal conglomerate is poorly sorted; thin beds of conglomerate and sandstone occur higher in the sequence.|30-APR-15
26240|Yandanooka Group|44144|6|Mentioned|p495, p522|Proterozoic|Proterozoic|Excluded from Perth Basin in this article; component of Pinjarra Orogen.||||||
26240|Yandanooka Group|48615|14|Not recorded|Fig.6|||(H50-6).||||||
26240|Yandanooka Group|48823|5|Briefly described|p24|||||||||
26240|Yandanooka Group|60556|5|Briefly described|p2 Fig. 2, p3|Proterozoic||||||||
26240|Yandanooka Group|61811|6|Mentioned|p6 Fig.4, p23.|||Striated and facetted clasts from this unit occur in the Nangetty Formation, 100 - 250 km to the north-northwest.||||||
26240|Yandanooka Group|62113|5|Briefly described|p620.|Neoproterozoic|Neoproterozoic|||Unit in Mullingarra Complex.|||Metasediments.|
26240|Yandanooka Group|62381|6|Mentioned|p2 Fig.2.|||||||||
26240|Yandanooka Group|63866|6|Mentioned|p183|||||||||
26240|Yandanooka Group|64580|4|Described|map legend||Neoproterozoic|Siltstone with abundant volcanic fragments, sandstone and conglomerate.||||||09-DEC-08
26240|Yandanooka Group|64635|6|Mentioned|p2 Fig.1, p5 Fig.4|||||||||
26240|Yandanooka Group|64722|5|Briefly described|Fig. 2 p3-6, p19|Neoproterozoic|Neoproterozoic|Siliciclastic rocks. Inferred to be late Neoproterozoic.||||Unconformably overlies Mullingarra Complex.||11-APR-12
26240|Yandanooka Group|65487|6|Mentioned|p2 Fig.1|Neoproterozoic|Mesoproterozoic|||||||10-FEB-14
26240|Yandanooka Group|67340|6|Mentioned|p7-8, 25, 35, 55|Proterozoic|Proterozoic|Basement to north Perth Basin. Thermal rock properties.||||||
26240|Yandanooka Group|69003|6|Mentioned|vi, p28, p54, p72|||||||||
26240|Yandanooka Group|69182|6|Mentioned|Ch2 p3|||Perth Basin.Pinjarra Orogen.||||||20-MAY-20
26240|Yandanooka Group|69583|6|Mentioned|p132|||Pinjarra Orogen.||||||
26240|Yandanooka Group|70796|4|Described|2_5m_interpgeop15_lut.csv|Mesoproterozoic|Mesoproterozoic|Of the Yandanooka Basin, Pinjarra Orogen. Affected by the Leeuwin Orogeny. See also 500k_interpgeop14_lut.csv.|ca 16001000 Ma (inferred)||||Siltstone with abundant volcanic fragments, sandstone and conglomerate.|
26240|Yandanooka Group|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Yandanooka Basin.||||||20-APR-20
26240|Yandanooka Group|71146|6|Mentioned|p16|Precambrian|Precambrian|Pinjarra Orogen.||||||
26240|Yandanooka Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
26240|Yandanooka Group|71269|5|Briefly described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Pinjarra Orogen. Of Yandanooka Basin. Events: Leeuwin Orogeny (780-515 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv.|1600-1000 Ma||||Siltstone with abundant volcanic fragments, sandstone and conglomerate|
26240|Yandanooka Group|71781|6|Mentioned|Plate 3|||||||||
26240|Yandanooka Group|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Yandanooka Basin.|||||Siltstone with abundant volcanic fragments, sandstone and conglomerate.|
24135|Yandanunyah Formation|22907|6|Mentioned|41|||||||||
24135|Yandanunyah Formation|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Of Tarcunyah Group, Officer Basin.||||||
24135|Yandanunyah Formation|23590|3|Fully described|p13|||Of Tarcunyah Group. Overlain by Wongarlong Formation. Underlain by Brownrigg Sandstone. Geol. prov: Officer Basin. Max. thickness: ~300 m.||||||24-JUL-07
24135|Yandanunyah Formation|23594|4|Described|p22|Neoproterozoic|Mesoproterozoic|Of Tarcunyah Group. Geological Province: Bangemall Basin. Max. thickness: >450 m.||||||
24135|Yandanunyah Formation|23746|4|Described|p26|Neoproterozoic|Mesoproterozoic|Of Tarcunyah Group. Previously Wandy Wandy Shale.||||||24-JUL-07
24135|Yandanunyah Formation|23760|4|Described|p28|Proterozoic|Proterozoic|Of Tarcunyah Group. Geological Province: Officer Basin.||||||
24135|Yandanunyah Formation|41669|2|Defined|Table 5|Precambrian?||||||||
24135|Yandanunyah Formation|42352|6|Mentioned|p29|||Part of Yeneena Group||||||
24135|Yandanunyah Formation|43055|4|Described|p28, Table 4|||Of the Yeneena Group.||||||24-JUL-07
24135|Yandanunyah Formation|43056|5|Briefly described|Map Legend|||Of the Yeneena Group.||||||24-JUL-07
24135|Yandanunyah Formation|43847|5|Briefly described|Map Legend||Proterozoic|||||||
24135|Yandanunyah Formation|44139|5|Briefly described|p277-280|Neoproterozoic|Neoproterozoic|(Williams 1989). 80 m. Dolomite, siltstone, shale. Western zone of Yeneena Basin. Conformably overlain by Choorun Formation.| | ||||06-MAR-18
24135|Yandanunyah Formation|44190|5|Briefly described|Map Legend||Proterozoic|||||||
24135|Yandanunyah Formation|44831|5|Briefly described|Map Legend||Proterozoic|||||||
24135|Yandanunyah Formation|50008|5|Briefly described|p46 Fig.3||Neoproterozoic|Of Tarcunyah Group. Geological Province: Officer Basin.||||||
24135|Yandanunyah Formation|60470|5|Briefly described|p4 Fig. 2|Neoproterozoic|Neoproterozoic|in Officer Basin, of Tarcunyah Group. Dolomite, siltstone, and shale||||||
24135|Yandanunyah Formation|62453|3|Fully described|p5 Fig. 3, 66|Cryogenian|Cryogenian|Of the Tarcunyah Group. Geological Province: Paterson Orogen. Conformably overlies Brownrigg Sandstone. Conformably overlain by Wongarlong Formation. Thickness: 300m. Siltstone, shale. ||||||
24135|Yandanunyah Formation|63417|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Tarcunyah Group. Geological Province: Officer Basin (Centralia Superbasin). Siltstone, shale, calcareous shale; locally stromatolitic carbonate.||||||23-JUL-07
24135|Yandanunyah Formation|64580|6|Mentioned|map legend|||Of Tarcunyah Group.||||||15-DEC-08
24135|Yandanunyah Formation|64777|5|Briefly described|p3 Fig.4 |Neoproterozoic|Neoproterozoic|||Of the Tarcunyah Group|||Dolomite, siltstone and shale.|
24135|Yandanunyah Formation|65454|4|Described|p7 Fig.3, p10, p30 Fig.A1b|Cryogenian|Cryogenian|Of Tarcunyah Group. Interbedded siltstone and shale, calcareous shale and minor silicified oolitic, laminated and locally strongly stromatolitic carbonate. Overlies Brownrigg Sandstone. Overlain by Wongarlong Formation.||||||
24135|Yandanunyah Formation|65725|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Tarcunyah Group. Underlain by Brownrigg Sandstone. Siltstone, shale, and fine-grained sandstone. Province: Officer Basin (Centralian Superbasin).||||||26-FEB-13
24135|Yandanunyah Formation|65826|5|Briefly described|p1, p11. |Neoproterozoic|Neoproterozoic| A transgressive, shallow-marine sequence deposited shorewards of carbonate build-ups, like the Waroongunyah Formation.  About 300 m thick.||Unit in Tarcunyah Group.||Conformably overlies Brownrigg Sandstone.|Interbedded purple, red, yellow and white siltstone and shale; commonly silicified calcareous shale; rare silicified, blue-white oolitic and laminated dolomite, stromatolitic in places.|23-MAY-16
24135|Yandanunyah Formation|67202|4|Described|p64-65, p125, p231|Neoproterozoic|Neoproterozoic|NW Officer Basin. 450m thick. Transgressive shallow-marine deposits.||Tarcunyah Group.||Conformably overlies Brownrigg Sandstone. Is overlain conformably by Wongarlong Formation.|Thick silicified shale, dolomite, calcareous shale and fine-grained sandstone.|
24135|Yandanunyah Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|NW Paterson Orogen.||Tarcunyah Group.||||
24135|Yandanunyah Formation|69167|4|Described|geologyp_lut.csv|Neoproterozoic|Neoproterozoic|||Tarcunyah Group|||Siltstone, shale, calcareous shale, locally stromatolitic carbonate.|
24135|Yandanunyah Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|Neoproterozoic|Neoproterozoic|||Unit of Tarcunyah Group.||||
24135|Yandanunyah Formation|69590|4|Described|GEOL_LUT_CSV files|Cryogenian|Neoproterozoic|Of Gibson Sub-basin, Officer Basin (Phase 1), Centralian Superbasin. Events: Delamarian Orogeny; Paterson Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|1000-635 Ma (Inferred)|Unit of Tarcunyah Group.|||Siltstone, shale, calcareous shale, locally stromatolitic carbonate|
24135|Yandanunyah Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||dololutite, shale, crystalline dolostone/dolomite|
24135|Yandanunyah Formation|72034|5|Briefly described|500k_interpgeop16_lut|Cryogenian|Tonian|Gibson Sub-basin, Officer Basin (Phase 1).||Tarcunyah Group|||Siltstone, shale, calcareous shale, locally stromatolitic carbonate.|
41175|Yandeearra Granodiorite|50370|5|Briefly described|Map Legend|Archean|Archean|Of Yule Granitoid Complex. Geological Province: Pilbara Craton||||||07-NOV-08
41175|Yandeearra Granodiorite|63372|4|Described|Map Legend|Archean|Archean|Of the Yule Granitoid Complex. Geological Province: East Pilbara Granite-Greenstone Terrane. Biotite-bearing granodiorite, weakly to strongly foliated; metamorphosed.||||||07-NOV-08
41175|Yandeearra Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite|
41175|Yandeearra Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|||Sisters Supersuite|||Biotite granodiorite, weakly to strongly foliated; metamorposed.|
35993|Yangibana Granite|50216|5|Briefly described|p213|Paleoproterozoic|Paleoproterozoic|Of the northern Gascoyne Complex. Age: 1660+/-9 Ma (Nelson, 2002).||||||07-NOV-08
35993|Yangibana Granite|50225|5|Briefly described|p388, p397|Paleoproterozoic|Paleoproterozoic|Age: c.1660Ma (Nelson, 2002).||||||07-FEB-11
35993|Yangibana Granite|50292|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Complex.  Age: 1660Ma.||||||07-NOV-08
35993|Yangibana Granite|61262|2|Defined|p459 App., p447 Fig. 4.|Paleoproterozoic|Paleoproterozoic|Of Durlacher Supersuite. Biotite-musc syenogranite to monzogranite; 2 plutons EDMUND 1:100 000; dykes and veins intrude Pooranoo Metamorphics and Pimbyana Granite. Unconformably underlies Edmund Gp sediments. Age:1659+/-10Ma, 1660+/-9Ma U-Pb.Type locality||||||17-FEB-09
35993|Yangibana Granite|63470|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Durlacher Supersuite. Geological Province: Gascoyne Complex. Equigranular to weakly porphyritic, medium-grained biotite-muscovite(-tourmaline) monzogranite with abundant inclusions of metasedimentary rock or porphyritic granodiorite.||||||17-FEB-09
35993|Yangibana Granite|63866|4|Described|p160, p162|Statherian|Statherian|Emplaced during the Mangaroon Orogeny. SHRIMP ages derived from Nelson, 2002.|1659 +/- 10 Ma and 1660 +/- 9 Ma (SHRIMP U-Pb_|Durlacher Supersuite||Intrudes the Pooranoo Metamorphics.||
35993|Yangibana Granite|63869|5|Briefly described|p19-20, p29, Plate 1|Paleoproterozoic|Paleoproterozoic|Pearson (1996); Martin et al.,(2002). SHRIMP U-Pb zircon crystallisation ages (GSWA, 2005).|1659 +/- 10 Ma and 1660 +/- 9 Ma.|Unit in Durlacher Supersuite.||Intrudes Pimbyana Granite.|A massive, leucocratic, medium-grained biotite-muscovite syenogranite to monzogranite, equigranular to slightly porphyritic.|
35993|Yangibana Granite|66299|3|Fully described|p172, pp264-265.|Paleoproterozoic|Paleoproterozoic|Gascoyne province. |1660 +/- 9 Ma.|Unit in Durlacher Supersuite.||Intrudes Gooche Gneiss and Pimbyana Granite.|Equigranular to locally weakly porphyritic, medium-grained biotite-muscovite monzogranite; locally contains tourmaline; may contain inclusions of metasedimentary rock or porphyritic granodiorite.|
35993|Yangibana Granite|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Age derived from biotite-muscovite granite sample (169055.1.pdf)|1659 Ma +/- 10 Ma (SHRIMP)|Durlacher Supersuite|||Equigranular to locally weakly porphyritic, medium-grained biotite--muscovite monzogranite; locally contains tourmaline and may contain abundant inclusions of metasedimentary rock or porphyritic granodiorite|
35993|Yangibana Granite|69237|5|Briefly described|p1, p3, p12-13|||Gascoyne Province.|1660-1659 Ma.|Durlacher Supersuite.||Is intruded by the Gifford Creek Ferrocarbonatite Complex.||
35993|Yangibana Granite|69546|5|Briefly described|p100,105,111|Statherian|Statherian|Geological province: Gascoyne Province. Intruded by Gifford Creek Ferrocarbonite Complex.||Unit of Durlacher Supersuite.||||
35993|Yangibana Granite|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_geologyl_lut.csv, 100k_interpgeop_lut.csv, 169055.1.pdf, 169059.1.pdf|1660-1659 Ma||||Equigranular to locally weakly porphyritic, medium grained biotite-muscovite monzogranite and granite; locally contains tourmaline and abundant inclusions of abundant inclusions of metasedimentary rock or porphyritic granodiorite.|
35993|Yangibana Granite|70814|5|Briefly described|p3, p49, p69|Statherian|Statherian||1675-1660 Ma|Durlacher Supersuite||Unconformably overlain by the Edmund Group.||
35993|Yangibana Granite|71869|5|Briefly described|p8, app p15|||Capricorn Orogen.|1659 +/- 10 Ma (igneous crystallisation age)|Durlacher Supersuite|||Biotite-muscovite monzogranite.|
35993|Yangibana Granite|74493|5|Briefly described|p3 Fig.2, p6|||||||Cut by Gifford Creek Carbonatite Complex||
35993|Yangibana Granite|74494|5|Briefly described|p1008-1009, p1012, p1014, p1019, p1022|Mesoproterozoic|Mesoproterozoic|Intruded by ironstone dykes of the Gifford Creek Carbonatite Complex.||Durlacher Supersuite||Intruded by Gifford Creek Carbonatite Complex||
36022|Yannery Granite|24192|5|Briefly described|p856|||Geological Province: Pilbara Craton.||||||15-DEC-08
36022|Yannery Granite|24352|5|Briefly described|Map legend|Archean|Archean|Age: c.2925Ma.   Fine to medium-grained, nonfoliated monzogranite; amphibole replaced by chlorite; anomalously magnetic.  Geological Province: Pilbara Craton||||||07-NOV-08
36022|Yannery Granite|24353|5|Briefly described|p9 Fig.5|Archean|Archean|Intrudes the Whundo Group. Underlain by North Whundo Intrusion. Geological Province: Pilbara Craton.||||||07-NOV-08
36022|Yannery Granite|63441|5|Briefly described|p12 tb. 2|Archean|Archean|Now part of the Radley Suite (Sisters Supersuite). In contact with the North Whundo Intrusion. Geological province: Pilbara Craton.||||||07-FEB-11
36022|Yannery Granite|64174|5|Briefly described|Map legend|Archean|Archean|Part of the Radley Suite (Sisters Supersuite). Age: c.2930Ma.  Hornblende granite;massive; iron oxide and hornblende replaced by chlorite.||||||07-NOV-08
36022|Yannery Granite|64580|4|Described|map legend||Mesoarchean|Of Radley Suite. Hornblende granite; massive; iron oxide and hornblende replaced by chlorite.||||||15-DEC-08
36022|Yannery Granite|67201|5|Briefly described|p16-17 Fig.9|Archean|Archean|Pilbara Craton. In Roebourne-Karratha area.||Radley Suite|||Hornblende granite; massive; iron oxide and hornblende replaced by chlorite.|
36022|Yannery Granite|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological Province: West Pilbara Granite-Greenstone Terrane, Central Pilbara Tectonic Zone, and southwest Pilbara inlier, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.||Unit of Radley Suite.|||Hornblende granite; massive; iron oxide and hornblende replaced by chlorite|
36022|Yannery Granite|70775|5|Briefly described|p15, p66, p78|Mesoarchean|Mesoarchean|Pilbara Craton.|2930 +/- 4 Ma (Smith, 2003)|Radley Suite|||Hornblende granite; massive; iron oxide and hornblende replaced by chlorite.|
36022|Yannery Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
36022|Yannery Granite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||2930+/-4 Ma|Radley Suite|||Hornblende granite; massive; iron oxide minerals and hornblende replaced by chlorite; metamorphosed.|
82206|Yapukarninjarra Formation|73345|3|Fully described|p224, p226-231|Paleozoic|Paleozoic|Newly defined. Canning Basin, Barnicarndy Graben. Named after consultation with the Western Desert Lands Aboriginal Corporation (WDLAC) and is a Martu word translated as 'rock underground'. Type section is between 2443 and 2585 m in Barnicarndy 1. Thickness of 142 m. The lower boundary is a major angular unconformity overlying weakly metamorphosed dolomites interpreted as part of the Neoproterozoic Yeneena Basin. Constitutes the oldest identified formation in the Canning Basin. May extend downward into the upper Cambrian. Separated from the overlying Fly Flat Member based on their different detrital zircon signatures. Detrital signature closely matches a red sandstone unit sampled from the base of Samphire Marsh 1.||||Conformably overlain by Nambeet Formation (Fly Flat Member).|Red and grey, medium- to coarse-grained quartz arenites with rare mottled bioturbation, local argillaceous sandy siltstone interbeds and poorly sorted arkose at the very base.|
70138|Yareweeree Boninite Member|63441|2|Defined|p5 Tb.1, p29|Archean|Archean|Of Bookingarra Formation (Croydon Group, Pilbara Supergroup). Geological province: Mallina Basin, Pilbara Craton. Subvolcanic intrusions.||||||07-FEB-11
70138|Yareweeree Boninite Member|63538|5|Briefly described|p32, p33|Archean|Archean|Of Bookingarra Formation. Geological Province: Pilbara Craton.||||||07-FEB-11
70138|Yareweeree Boninite Member|70775|5|Briefly described|p29 tbl 5, p56|Mesoarchean|Mesoarchean|Mallina Basin.|c. 2950 Ma (Smithies et al 2004a)|||||
70138|Yareweeree Boninite Member|72668|6|Mentioned|p15||||||||Boninite like rocks.|
67833|Yaringa Formation|6943|5|Briefly described|p599, pp601-603, p605.|Silurian|Silurian|Formerly Yaringa Evaporite Member (Playford et al. 1975). Re-named in recognition of limited portion of Basin where evaporites dominate this unit. Llandovery conodonts at base of unit.||Unit in Dirk Hartog Group.||Overlies Ajana Formation. Is overlain by Coburn Formation, probably paraconformably.|Evaporites, sandstone.|
67833|Yaringa Formation|12729|5|Briefly described|p.5, 8, 10; Figs. 8, 9.|Early Silurian||Previously the Yaringa Evaporite Member of Playford et al. (1975). Up to 105 m thick.  Only age indication from a late Llandovery (Early Silurian) conodont fauna.||Dirk Hartog Group||Overlies the Ajana Formation (disconformably overlies the Marron Member), underlies the Coburn Formation.|Consists mainly of dolomite and evaporite rocks.|
67833|Yaringa Formation|14227|5|Briefly described|p7|Wenlockian|Wenlockian|Geological Province: Southern Carnarvon Basin. See also Yaringa Halite.||||||07-FEB-11
67833|Yaringa Formation|14228|5|Briefly described|p4, p5 fig2, p6 fig3, p14|Llandovery|Llandovery|Gascoyne Platform.||Dirk Hartog Group||Overlies Ajana Formation. Overlain by Coburn Formation.|Dolomite and evaporite (mostly halite).|
67833|Yaringa Formation|23572|4|Described|p10|Silurian|Silurian|Geological Province: Carnarvon Basin. Of the Dirk Hartog Group. Underlying Unit: Ajana Formation. Overlying Unit: Coburn Formation. Max. thickness: 105m.|||||Mainly dolomite and evaporite rocks, but with local sandstone.|20-JUN-13
67833|Yaringa Formation|23935|4|Described|p11 Fig.7|Ludlow|Llandovery|Of Dirk Hartog Group. Conformably overlies Ajana Formation. Conformably overlain by Coburn Formaiton. Geological Province: Southern Carnarvon Basin.||||||
67833|Yaringa Formation|49942|4|Described|p4 Fig.3, p9|Llandovery|Llandovery|Conformably overlies Ajana Formation. Conformably overlain by Coburn Formation. Of Dirk Hartog Group. Evaporitic and carbonate-siliclastic sediments. Geological Province: Gascoyne Platform.||||||
67833|Yaringa Formation|50084|4|Described|p77, 78|Silurian|Silurian|Conformably overlies Ajana Formation. Disconformably overlain by Coburn Formation. Thickness: 69 m. Of Dirk Hartog Group. Geological Province: Souther n Carnarvon Basin.||||||07-FEB-11
67833|Yaringa Formation|60384|6|Mentioned|p243 Fig 2a|Early Silurian||Southern Carnarvon Basin.||Of Dirk Hartog Group||||
67833|Yaringa Formation|60725|5|Briefly described|p28, p29 Fig.2. |Silurian|Silurian|Locally, moderate to good petroleum source potential.||Unit in Dirk Hartog Group.|||Carbonate-shales facies.|
67833|Yaringa Formation|65449|5|Briefly described|p34|Llandovery|Llandovery|Southern Carnarvon Basin. Age from conodonts and palynomorphs.||Dirk Hartog Group.||Overlies Ajana Formation.|Dolomite, dark grey shales, and beds of halite and anhydrite.|
67833|Yaringa Formation|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.||Dirk Hartog Group|||Includes blue/grey (light and dark banding) dolomitic claystone/siltstone.|
67833|Yaringa Formation|67200|6|Mentioned|p18 table 1, p46, p52, p56, app 2 p4|||Thermal conductivity of 4.13 W/mK||Dirk Hartog Group|||Dolomitic claystone and siltstone.|
67833|Yaringa Formation|69297|6|Mentioned|p249|Telychian|Telychian|Gascoyne Sub-basin of the Southern Carnarvon Basin. ||Dirk Hartog Group||Overlies the Ajana Formation. Overlain by the Coburn Formation.|Volcanics.|
67833|Yaringa Formation|71146|5|Briefly described|p6, p45|Wenlock|Wenlock|Southern Carnarvon Basin. Up to 105m thick.||Dirk Hartog Group||Overlies the Ajana Formation. Overlain by the Coburn Formation.|Halite, evaporite.|
33855|Yarlarweelor Gneiss Complex|12099|5|Briefly described|p676-7, 683-4, 686, Figs.1, 2, 8|Orosirian|Orosirian|Informal name? Shown in lower case in Fig 1. In fault contact with Bryah Group along the Billara and Kerba Faults. Developed when part of the Yilgarn Craton was pervasively deformed, metamorphosed and intruded by granite sheets and dykes (Sheppard and Swager, 1999). Also referred to as Yarlaweelor gneiss terrane in this paper|~1800 Ma.|||||04-MAR-13
33855|Yarlarweelor Gneiss Complex|22437|6|Mentioned|p852-3|||||||||
33855|Yarlarweelor Gneiss Complex|23781|5|Briefly described|p6|||||||||
33855|Yarlarweelor Gneiss Complex|24332|3|Fully described|p135 Fig. 1, p137|Paleoproterozoic|Archean|Mainly composed of banded leucocratic and mesocratic granitic gneisses, consisting of several interlayered rock types, repeatedly deformed and metamorphosed; most rock types are granitic.  Age: ca.1812Ma. Geol.Prov: Capricorn Orogen/ Yilgarn Craton||||||07-NOV-08
33855|Yarlarweelor Gneiss Complex|24544|5|Briefly described|p3|Paleoproterozoic|Archean|Age: 3300-1800 Ma. Geological Province: Narryer terrane, Yilgarn Craton.||||||07-NOV-08
33855|Yarlarweelor Gneiss Complex|50216|6|Mentioned|p202, 203|Archean|Archean|Fault-bounded block of the Narryer Terrane intruded and deformed by the Bertibubba Supersuite. See also p204 Fig.2, 211 Fig. 4.H9.||||||07-NOV-08
33855|Yarlarweelor Gneiss Complex|50217|6|Mentioned|p221 Fig.1, p222|||Structural term in this context.||||||
33855|Yarlarweelor Gneiss Complex|50218|5|Briefly described|p238 Fig. 1, p249|Paleoproterozoic|Archean|Granitic gneiss. Age: 3300-1800Ma. Locally deformed and intruded by Bertibubba Supersuite. In faulted contact with Bryah and Padbury Groups. Geological Province: Yilgarn Craton. See also Figs. 3 and 4, p241-42, p244.||||||07-FEB-11
33855|Yarlarweelor Gneiss Complex|50219|5|Briefly described|p258 Fig. 1|Paleoproterozoic|Archean|Age: 3300-1800Ma.||||||07-FEB-11
33855|Yarlarweelor Gneiss Complex|50220|6|Mentioned|p280|||Defined as part of the Narryer Gneiss Complex.||||||
33855|Yarlarweelor Gneiss Complex|50221|5|Briefly described|p296 Fig.1, p301|Paleoproterozoic|Archean|Structural term in this context. Granitic gneiss. Geological Province: Yilgarn Craton.||||||07-NOV-08
33855|Yarlarweelor Gneiss Complex|50222|6|Mentioned|p327|||See also Yarlaweelor Complex and Yarlaweelor Gneiss Complex.||||||
33855|Yarlarweelor Gneiss Complex|50226|6|Mentioned|p418|||Geological Province: northern edge of the Yilgarn Craton.||||||
33855|Yarlarweelor Gneiss Complex|50228|5|Briefly described|p491 Fig.10|||||||||
33855|Yarlarweelor Gneiss Complex|61262|5|Briefly described|p458 App.|||Intruded by Discretion Granite. Geological Province: Yilgarn Craton. See also p444.||||||
33855|Yarlarweelor Gneiss Complex|63246|6|Mentioned|p479||Archean|Geological province: Yilgarn Craton.||||||07-NOV-08
33855|Yarlarweelor Gneiss Complex|63866|5|Briefly described|p157, p160-p161|||Yilgarn Craton.||||Intruded by the Bertibubba Supersuite and the Moorarie Supersuite.||
33855|Yarlarweelor Gneiss Complex|63869|5|Briefly described|p10, p15, p16, p18|Archean|Archean|Yilgarn Craton. Adjacent to SE edge of Gascoyne Complex. D1n deformation dated c.1811 Ma; D2n fabric dated at 1797 +/- 4 Ma; intruded by granites c.1620 Ma.||||Is intruded by Durlacher Supersuite.||
33855|Yarlarweelor Gneiss Complex|64771|6|Mentioned|p7|||NE Narryer Terrane. Affected by the Capricorn Orogeny.||||||
33855|Yarlarweelor Gneiss Complex|65830|6|Mentioned|p1 Fig.1, p24-25|Archean||Intensely deformed and metamorphosed margin of the Yilgarn Craton.||||Intruded by the Durlacher Supersuite.||
33855|Yarlarweelor Gneiss Complex|66106|6|Mentioned|p44|||Underwent Capricorn Orogeny tectonism (high-grade metamorphism and granitoid magmatism) between 1812 Ma and 1800 Ma.||||||
33855|Yarlarweelor Gneiss Complex|66299|4|Described|p30, p34, pp116-120.|Paleoproterozoic|Archean|Component of Glenburgh Terrane, basement to Gascoyne Province. Mostly reworked granitic gneiss. Deformed during Capricorn Orogeny.|c.3298-1813 Ma.||||Granitic gneisses, interleaved with lenses and strips of fine- and medium-grained amphibolite (metamorphosed dolerite dykes and veins); metamorphosed banded iron-formation; quartzite; calc-silicate gneiss.|
33855|Yarlarweelor Gneiss Complex|66427|6|Mentioned|p40 Fig.1 |||Mis-spelt as Yarlaweelor in Fig.1 and appears as Yarlaweelor Cx in Tb.1. Granite intrusions in Narryer Terrane.||||||
33855|Yarlarweelor Gneiss Complex|66887|5|Briefly described|p2-6, p22|Archean|Archean|Imbricated slices of reworked Yilgarn Craton located in Errabiddy Shear Zone (at southern boundary of Glenburgh Terrane). Southern Gascoyne Province.||||Intruded by Bertibubba Supersuite.|Granitic rocks and gneisses.|
33855|Yarlarweelor Gneiss Complex|66950|5|Briefly described|p6, p9 Fig.8, p12, p13, pp17-19, p23|Archean|Archean|Contains gneissic fabrics, upright folds, and metamorphic assemblages up to amphibolite facies.||||Intruded by the Durlacher Supersuite.|Comprises granite-greenstone rocks.|
33855|Yarlarweelor Gneiss Complex|67843|5|Briefly described|p2 Fig.1, p4 Fig.2, p12, p39.|Archean|Archean|Parts of this unit and the Narryer Terrane are interleaved with rocks of the Glenburgh Terrane along the Errabiddy Shear Zone.||||Is intruded by Bertibubba Supersuite.||
33855|Yarlarweelor Gneiss Complex|68055|6|Mentioned|p76 Fig.1, p87|||Capricorn Orogen, northern Yilgarn Craton.|||||Amphibolite-grade metamorphic assemblages; gneissic fabrics and upright folds.|
33855|Yarlarweelor Gneiss Complex|68123|6|Mentioned|p28-30, 32, 34-38, 42|Archean|Archean|Yilgarn Craton. Includes zircons aged 3000 Ma, possibly derived from the Narryer Gneiss Complex. Detrital zircon age peak at c.3280 Ma.|c.3300-1800 Ma.||||Granites, granitic gneiss and supracrustal rocks.|
33855|Yarlarweelor Gneiss Complex|69003|5|Briefly described|p26|Paleoproterozoic|Paleoproterozoic|Southernmost Gascoyne Province. Magmatic activity was accompanied by metamorphisn and deformation.|c.1820 - c.1810 Ma.|||||
33855|Yarlarweelor Gneiss Complex|69080|5|Briefly described|p684, p686 Fig.4, p688-689|||Narryer Terrane, Yilgarn Craton. Strongly deformed by the 1820-1770 Ma Capricorn Orogeny.|||||Metamorphosed and deformed Narryer Terrane granites; intruded by c.1800 Ma granite and pegmatite.|
33855|Yarlarweelor Gneiss Complex|69166|6|Mentioned|183212.1.pdf|||||||Intruded by Moorarie Supersuite||
33855|Yarlarweelor Gneiss Complex|69387|5|Briefly described|p2-5, p7, p9, p11, p13, p21-23, p40|||See also p42-43, p45, p48-50. Encompasses the N and NE margins of the Narryer Terrane, which were strongly reworked, with extensive granite emplacement, during the 1820-1770 Ma Capricorn Orogeny. Deformation detailed. SG and magnetic susceptibility values given. Fuzzy prospectivity models.||||Is intruded by Durlacher Supersuite.||
33855|Yarlarweelor Gneiss Complex|69583|5|Briefly described|p57, p130, p132, p140-141, p147-148|Paleoproterozoic|Paleoproterozoic|See also p155-156; Plates 2, 3. NE Narryer Terrane. Affected by the Paleoproterozoic Capricorn Orogeny.|3352-1813 Ma.||Warrigal Gneiss.||Foliated metagranite.|
33855|Yarlarweelor Gneiss Complex|69596|6|Mentioned|p2, p5, p13|||Yilgarn Craton, Capricorn Orogen.||||||
33855|Yarlarweelor Gneiss Complex|70795|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoarchean|West Australian Craton|3298-1813 Ma||||leucocratic granitic gneiss, mesocratic granitic gneiss, foliated, porphyritic biotite metamonzogranite with coarse round phenocrysts of K-feldspar|
33855|Yarlarweelor Gneiss Complex|70826|6|Mentioned|p8, p9|Paleoproterozoic|Paleoproterozoic|||||Intruded by the Moorarie Supersuite.||12-MAY-20
33855|Yarlarweelor Gneiss Complex|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoarchean|Narryer Terrane. Three unnamed subunits identified. Granite gneiss; reworked during the Paleoproterozoic, max age ~3352 Ma, min 1813+/-8 Ma. Leucocratic granitic gneiss; derived from 3300-2640 Ma biotite granite and granitic gneiss, and sheets and veins of coarse-grained granite and pegmatite (P_-MO-mgp); deformed and metamorphosed at 1810 Ma, Max age 3298+/-6 Ma, min 1813+/-8 Ma. Metagranitic rock.|max age ~3352 Ma, min 1813+/-8 Ma.||||Granite gneiss. Leucocratic granitic gneiss. Metagranitic rock.|
33855|Yarlarweelor Gneiss Complex|72259|6|Mentioned|p3|Neoarchean|Archean||ca. >2600 Ma|||||
33855|Yarlarweelor Gneiss Complex|73102|5|Briefly described|p3|||Yilgarn Craton.|||||Metamorphosed and deformed Narryer Terrane Granites; intruded by c.1800 Ma granite and pegmatite.|
33855|Yarlarweelor Gneiss Complex|73214|5|Briefly described|p974 Fig.1, 975-976, 980, 988|Archean|Archean|Occhipinti et al. (2001). Yilgarn Craton.|||Kerba Granite.|||
33855|Yarlarweelor Gneiss Complex|73442|5|Briefly described|p3|||Yilgarn Craton.|||||Metamorphosed and deformed Narryer Terrane granites; intruded by c.1800 Ma granite and pegmatite.|
31763|Yarra Yarra Granite|23569|4|Described|p5 Tb. 1|Archean|Archean|Of the Narryer Terrane.   Coarse-grained, equigranular, leucocratic granulite-facies monzogranite||||||07-NOV-08
31763|Yarra Yarra Granite|23574|5|Briefly described|Map Legend|Archean|Archean|Underlying unit Churla Granite.||||||07-NOV-08
31763|Yarra Yarra Granite|23576|5|Briefly described|Map Legend|Archean|Archean|Underlying unit Churla Granite||||||07-NOV-08
31763|Yarra Yarra Granite|23577|5|Briefly described|Map Legend|Archean|Archean|Underlying unit Churla Granite.||||||07-NOV-08
31763|Yarra Yarra Granite|24114|5|Briefly described|p5 Fig.4|Archean|Archean|Geological Province: Yilgarn Craton. Age: c. 2620 Ma.||||||07-NOV-08
31763|Yarra Yarra Granite|43835|5|Briefly described|Map Legend|Archean|Archean|Age about 2620Ma.||||||07-NOV-08
31763|Yarra Yarra Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzonite|
31763|Yarra Yarra Granite|73526|6|Mentioned|p2 Fig.1, p4|||Inferred to comprise large tracts of the northwestern Narryer Terrane (Myers, 1997b).||||||
75914|Yarrabubba Monzogranite|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane||Walganna Suite|||Coarse-grained, muscovite monzogranite; typically with large, round quartz phenocrysts; local pegmatite patches|
75914|Yarrabubba Monzogranite|69628|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton||Walganna Suite|||Coarse-grained, muscovite monzogranite; typically with large, round quartz phenocrysts; local pegmatite patches.|
75914|Yarrabubba Monzogranite|70796|5|Briefly described|100k_geologyp_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton. See also 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|2647 +/ 11 Ma (isotopic)|Walganna Suite|||Coarsegrained, muscovite monzogranite; typically with large, round quartz phenocrysts; local pegmatite patches|
75914|Yarrabubba Monzogranite|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.|2650+\-15 Ma|Unit of Walganna Suite.|||Medium- to coarse-grained, muscovite--albite monzogranite; contains veins of quartz, pseudotachylite and muscovite-bearing pegmatite; quartz grains show microscopic planar deformation features (PDFs)|
79248|Yarragadee Sequence|69297|6|Mentioned|p202, p204, p206|||Perth Basin. Sandstones and siltstones were deposited in a fluvial-deltaic environment. Good TOC and potential for both oil and gas generation. See also p207, p209, p223, p225, p236, p238.||||Overlies the Cadda Sequence.|Sandstones and siltstones.|
79248|Yarragadee Sequence|70097|5|Briefly described|p3, p4-5|Late Jurassic|Late Jurassic|Rifting, offshore northern Perth Basin. Houtman Sub-basin. Early Cretaceous intrusive rocks interpreted.|||||Fluvio-deltaic sandstones and siltstones were deposited in the lower part of the Yarragadee Sequence, followed by coarse-grained fluvial sediments.|20-OCT-15
29187|Yarraloola Conglomerate|12471|5|Briefly described|p474.|Early Cretaceous|Early Cretaceous|Oil and gas shows occurred in this unit during a 1966 seismic survey and subsequently. Deposited after continental break-up; formed a sub-horizontal blanket with Nanutarra Formation over older strata. Has excellent porosity and permeability.|||||Polymictic conglomerate.|
29187|Yarraloola Conglomerate|13615|3|Fully described|p4-p5, p12, p15, p18|Berriasian|Tithonian|Peedamullah Shelf. Generally <50m thick. Spores/Pollen Zone and Dinoflagellate zones provided. Deposited in a fluviatile floodplain. Rocks assigned to this formation have been reinterpreted as belonging to the Flacourt Formation. Type section occurs 11km southeast of Yarraloola Homestead; 21deg37'30"S 115deg57'10"E. Contains sparse bivalve fauna, common wood and leaves. Deposited in a fluvial to alluvial fan setting. See also p35, p43, p45-p46, p51, p61-p62, p73, p83, p102.||Of Barrow Group||Along with Nannutarra Formation, likely time equivalent to the Flacourt Formation.|Pebble to cobble conglomerate, poorly sorted sandstone and minor siltstone.|01-MAY-19
29187|Yarraloola Conglomerate|23311|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|Of Winning Group.||||||
29187|Yarraloola Conglomerate|23325|6|Mentioned|map legend|Cretaceous|Cretaceous|||||||
29187|Yarraloola Conglomerate|23403|4|Described|p8|||||||||
29187|Yarraloola Conglomerate|23575|5|Briefly described|Map Legend|Mesozoic|Mesozoic|||||||
29187|Yarraloola Conglomerate|23726|5|Briefly described|p72|Early Cretaceous|Early Cretaceous|Overlying unit Muderong Shale. Geological Province: Carnarvon Basin.||||||
29187|Yarraloola Conglomerate|23815|5|Briefly described|p295|Early Cretaceous|Early Cretaceous|Geological Province: Carnarvon Basin. Underlying unit: Nanutarra Formation.||||||27-APR-05
29187|Yarraloola Conglomerate|24059|6|Mentioned|p132|||||||||
29187|Yarraloola Conglomerate|24573|5|Briefly described|p671 Fig.2|Cretaceous|Cretaceous|Geological Province: Pilbara Craton||||||
29187|Yarraloola Conglomerate|32648|6|Mentioned|p32|||Meocomian||||||
29187|Yarraloola Conglomerate|33165|6|Mentioned|Chart|||Correlation chart only||||||
29187|Yarraloola Conglomerate|33450|6|Mentioned|p10|||Fig.5||||||
29187|Yarraloola Conglomerate|33540|6|Mentioned|p890|||||||||
29187|Yarraloola Conglomerate|34066|6|Mentioned|p12|||||||||
29187|Yarraloola Conglomerate|34840|6|Mentioned|p68|||||||||
29187|Yarraloola Conglomerate|35144|6|Mentioned|p4|||||||||
29187|Yarraloola Conglomerate|35282|6|Mentioned|p25|||||||||
29187|Yarraloola Conglomerate|36890|3|Fully described|p295|||||||||
29187|Yarraloola Conglomerate|36902|6|Mentioned|p22|||||||||
29187|Yarraloola Conglomerate|37016|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
29187|Yarraloola Conglomerate|37422|6|Mentioned|p6|||||||||
29187|Yarraloola Conglomerate|37633|6|Mentioned|p14|||||||||
29187|Yarraloola Conglomerate|38482|5|Briefly described|p23|||See also p22.||||||01-MAY-19
29187|Yarraloola Conglomerate|39158|4|Described|p38|||See also p38.||||||01-MAY-19
29187|Yarraloola Conglomerate|39427|4|Described|Table 1|||||||||
29187|Yarraloola Conglomerate|39757|6|Mentioned|p1605|||||||||
29187|Yarraloola Conglomerate|40617|6|Mentioned|p18|||||||||
29187|Yarraloola Conglomerate|40987|4|Described|p35|||||||||
29187|Yarraloola Conglomerate|41271|3|Fully described|p141|||||||||
29187|Yarraloola Conglomerate|41438|6|Mentioned|p108|||||||||
29187|Yarraloola Conglomerate|41441|6|Mentioned|p153|||See also Fig.6||||||
29187|Yarraloola Conglomerate|41443|6|Mentioned|p164|||||||||
29187|Yarraloola Conglomerate|41446|3|Fully described|p215|||||||||
29187|Yarraloola Conglomerate|42116|4|Described|p31|||||||||
29187|Yarraloola Conglomerate|42190|6|Mentioned|Fig.4 Map|||||||||
29187|Yarraloola Conglomerate|42598|3|Fully described|P 95, P 37|Neocomian||||||||
29187|Yarraloola Conglomerate|43442|6|Mentioned|p61|||Northern Carnarvon Basin||||||
29187|Yarraloola Conglomerate|44477|4|Described|p.15, Table 1||Mesozoic|SF/50-6.||||||
29187|Yarraloola Conglomerate|44478|14|Not recorded|map legend||Cretaceous|||||||
29187|Yarraloola Conglomerate|44481|5|Briefly described|map legend||Cretaceous|||||||
29187|Yarraloola Conglomerate|63432|5|Briefly described|p736 Fig. 2|Cretaceous|Cretaceous|||||||07-FEB-11
29187|Yarraloola Conglomerate|64973|6|Mentioned|p504|||Misspelt or obsolete name. The original use of the name was not intended to be formal.||||||16-JUN-09
29187|Yarraloola Conglomerate|65194|5|Briefly described|p16 Fig.2.4, p99, p100 Fig.2.24, p113|Cretaceous|Cretaceous|Deposited in a basal channel in eroded Wittenoom Dolomite. Fluvial deposits in Fortescue-Robe Palaeovalley. Is overlain unconformably by Robe (Pisolite) Formation and Trealla Limestone.||||||07-APR-16
29187|Yarraloola Conglomerate|67200|5|Briefly described|p8 fig 6, p54|Cretaceous|Cretaceous|Thermal conductivity of 2.10 W/mK||||Overlain by Muderong Shale|Parallel and trough cross bedded, interbedded sandstone, siltstone and conglomerate.|
29187|Yarraloola Conglomerate|69166|6|Mentioned|500k_geologyp08_lut.csv|Cretaceous|Cretaceous||||Includes Nanutarra Formation|||
29187|Yarraloola Conglomerate|69538|5|Briefly described|p522 Fig.5, p526 Fig.7, p534|Cretaceous|Cretaceous||||||Valley sediment with rare martite-goethite ore pebbles.|
29187|Yarraloola Conglomerate|70795|6|Mentioned|100k_geologyp_lut.csv, |Aptian|Berriasian|Also 2_5m_interpgeop15_lut.csv, 100k_interpgeop_lut.csv|||||Poorly sorted sandstone (in places glauconitic) cobble to boulder conglomerate and silstone.|
29187|Yarraloola Conglomerate|70826|6|Mentioned|p7 tbl 4|Cretaceous|Cretaceous|Northern Carnarvon Basin.||||||
29187|Yarraloola Conglomerate|71273|5|Briefly described|Map legend.|Cretaceous|Cretaceous||145-113 Ma.||||Polymictic cobble to small boulder conglomerate, lesser sandstone; minor siltstone.|
29187|Yarraloola Conglomerate|71808|6|Mentioned|p53|Cretaceous|Cretaceous|||||||
29187|Yarraloola Conglomerate|72034|5|Briefly described|500k_interpgeop16_lut|Early Cretaceous|Early Cretaceous|Northern Carnarvon Basin. Age inferred.|||||Polymictic cobble to small boulder conglomerate, lesser sandstone; minor siltstone.|
29187|Yarraloola Conglomerate|72758|5|Briefly described|p8 Tb.1, p54.|Cretaceous|Cretaceous|Occuring as small mesas and buttes in northwest Wyloo mapsheet area.||||Unconformably overlies Mount Minnie Group|Includes ferruginous sandstone and conglomerate, some fissile mudstone.|
29187|Yarraloola Conglomerate|73574|5|Briefly described|p761-763|Valanginian|Tithonian|Western Hamersley Province and North Carnarvon Basin. Substantial variations in thickness. Present distribution appears to define ancient river courses. Early Valanginian minimum age.||||Unconformably overlies Hamersley Group, possible onshore correlative of Barrow Group.|Polymict fluvial conglomerate, in places contains clasts derived from the Hamersley Group; commonly ferruginous and contains plant fossils.|
80136|Yarraquin granite|69583|6|Mentioned|p42, p44|||Large, composite pluton associated with migmatites; shows widespread evidence of deformation during and immediately after crystallisation. See also Yarraquin pluton p115-116, 113, 114, 119, 121.|||||Mainly high temperature granitic gneiss, including numerous xenoliths of mafic gneiss and paragneiss.|27-SEP-17
80136|Yarraquin granite|69744|6|Mentioned|p255, 259, 262|||Murchison Domain, Youanmi Terrane. c.100km x 50km. More commonly referred to as the Yarraquin pluton.|c.2710-2795 Ma.||||Composite syntectonic pluton associated with migmatites.|
30540|Yarri Monzogranite|43205|5|Briefly described|map legend||Archean|||||||07-NOV-08
30540|Yarri Monzogranite|43593|4|Described|Fig.3,p6,15|||||||||
30540|Yarri Monzogranite|44203|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
30540|Yarri Monzogranite|60076|5|Briefly described|p46 App. 1|||[Agmya]   Biotite monzogranite; K-feldspar phenocrysts.||||||
30540|Yarri Monzogranite|64775|5|Briefly described|p3-1,2|||Age: predates Galvalley Monzogranite. Gold rich.|||||Porphyritic biotite monzogranite. Coarse-grained and pervasively foliated.|30-MAR-12
30540|Yarri Monzogranite|65264|5|Briefly described|p48 Appdx. 1|Archean|Archean|Biotite monzogranite; K-feldspar phenocrysts; pervasive foliation and quartz veins are folded locally.||||||07-FEB-11
30540|Yarri Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton. Data migrated from OZCHRON1. Original comment: 'Most of the zircon in this rock is interpreted as having crystallised from this monzogranite. However, it has extremely high U, which has produced substantial Pb loss. 6 of the 7 low-U grains yield an age of 2717+/-19 Ma, which probably dates inheritance.'|2717+/-19 Ma U/Pb SHRIMP||||Biotite monzogranite; K-feldspar phenocrysts; pervasive foliation and quartz veins are folded locally.|07-AUG-15
30540|Yarri Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|See also GA_geochron.csv and GA_rocks.csv|2717 +/- 19 Ma (SHRIMP).||||Fine- to medium-grained, equigranular monzogranite. Biotite monzogranite; K-feldspar phenocrysts; pervasive foliation and quartz veins are folded locally.|
30540|Yarri Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
30540|Yarri Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. See 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|||||Biotite monzogranite; K-feldspar phenocrysts; pervasive foliation and quartz veins are folded locally|
33176|Yeelingee Member|22905|6|Mentioned|p53|||Of Daniels (1970).||||||20-MAY-04
33176|Yeelingee Member|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Irregully Formation.||||||
33176|Yeelingee Member|24183|6|Mentioned|p14|||Correlated with the Terrys Camp Member||||||
33176|Yeelingee Member|34066|4|Described|p11, Table 1|Mesoproterozoic|Mesoproterozoic|Of Irregully Formation. Mid.Prot.||||||
33176|Yeelingee Member|36884|4|Described|p152|||||||||
33176|Yeelingee Member|40089|5|Briefly described|p24|||||||||
33176|Yeelingee Member|44481|5|Briefly described|map legend||Mesoproterozoic|Part of Irregully Formation.||||||
33176|Yeelingee Member|72758|5|Briefly described|p8-9 Tb.1, p50, p52, p59.|||210 m (p8) or 120 m (p52) thick. Part of the 2800m thick Irregully Formation.  Lateral equivalent of Wannery Member near Mount Florry.||Irregully Formation||Conformably overlies Weewoddie Dolomite Member, overlies Chubilyer Member. Laterally equivalent to Wannery Member.|Finely laminated mudstone, sandstone, and thin dolomite beds.|
25669|Yeelirrie Member|41199|4|Described|p12|||Reserved as Yeelirrie. Of Menzies Formation.||||||
25669|Yeelirrie Member|43065|6|Mentioned|p93|||of Menzies Formation||||||
31375|Yeneena Supergroup|22907|6|Mentioned|41|||||||||
31375|Yeneena Supergroup|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Yeneena Basin.||||||
31375|Yeneena Supergroup|23414|5|Briefly described|Map Legend|Neoproterozoic|Mesoproterozoic|Yeneena Basin||||||
31375|Yeneena Supergroup|23575|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
31375|Yeneena Supergroup|23585|5|Briefly described|p21|||Geological Province: Yeneena Basin.||||||
31375|Yeneena Supergroup|23590|2|Defined|p8, p22 Appendix 2|Neoproterozoic|Mesoproterozoic|Previously Yeneena Group. Age: <1300 to >850 Ma (poor age constraints). Underlying unit Rudall Complex. Max. thickness ~1200 m.||||||
31375|Yeneena Supergroup|23594|4|Described|p21|||Geological Province: Bangemall Basin.||||||
31375|Yeneena Supergroup|23602|4|Described|p15|||||||||
31375|Yeneena Supergroup|23729|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province:  Yeneena Basin.||||||
31375|Yeneena Supergroup|23730|4|Described|p9|Neoproterozoic|Mesoproterozoic|Geological Province: Yeneena Basin.||||||
31375|Yeneena Supergroup|23742|4|Described|p6||Mesoproterozoic|Geological Province: Paterson Orogen.||||||
31375|Yeneena Supergroup|23745|4|Described|p16|Proterozoic|Proterozoic|||||||
31375|Yeneena Supergroup|23746|4|Described|p23|Proterozoic|Proterozoic|Geological Province: Pilbara Craton.||||||
31375|Yeneena Supergroup|23758|4|Described|p5|Neoproterozoic|Mesoproterozoic|Geological Province: Yeneena Basin.||||||
31375|Yeneena Supergroup|23760|4|Described|p21|Proterozoic|Proterozoic|Geological Province: Yeneena Basin.||||||
31375|Yeneena Supergroup|23900|4|Described|p1536|Proterozoic|Proterozoic|Unconformably overlies the Rudall Complex. Geological Province: Paterson orogen.||||||
31375|Yeneena Supergroup|24025|4|Described|p15|Neoproterozoic|Neoproterozoic|Formerly "Yeneena Group".  Geological Province: Pilbara Craton.||||||
31375|Yeneena Supergroup|24110|5|Briefly described|Plate 1|Proterozoic|Proterozoic|Geological Province: Yeneena Basin.||||||
31375|Yeneena Supergroup|24194|4|Described|p898 Fig.1|||Comprises the Throssell and Lamil Groups. Underlying Unit: Rudall Complex. Geological Province: Yeneena Basin||||||
31375|Yeneena Supergroup|43561|6|Mentioned|p1440|||Approx. 1300-1100 Ma.  Variation on Yeneena Group||||||
31375|Yeneena Supergroup|43847|5|Briefly described|Map Legend||Proterozoic|||||||
31375|Yeneena Supergroup|43848|5|Briefly described|Map Legend||Proterozoic|||||||
31375|Yeneena Supergroup|43849|5|Briefly described|Map Legend||Proterozoic|||||||
31375|Yeneena Supergroup|43856|5|Briefly described|Map Legend||Proterozoic|||||||
31375|Yeneena Supergroup|44111|6|Mentioned|p.56 Fig. 1|||||||||
31375|Yeneena Supergroup|44189|5|Briefly described|Map legend||Proterozoic|||||||
31375|Yeneena Supergroup|44190|5|Briefly described|Map Legend||Proterozoic|||||||
31375|Yeneena Supergroup|44831|5|Briefly described|Map Legend||Proterozoic|||||||
31375|Yeneena Supergroup|44866|5|Briefly described|Map Legend||Neoproterozoic|||||||
31375|Yeneena Supergroup|49895|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Geological Province: Paterson Orogen. Contains both the Throssell and Lamil Groups. See also p2 Fig.1.||||||
31375|Yeneena Supergroup|49911|5|Briefly described|Map legend|Neoproterozoic|Mesoproterozoic|Age: >900Ma.  Geological Province: Yeneena Basin.||||||
31375|Yeneena Supergroup|50436|5|Briefly described|p4.1|||Used interchangeably with Yeneena Group. Includes: Isdell Formation, Malu Quartzite, Telfer Formation, Puntapunta Formation, Wilki Quartzite, Kaliranu Beds.||||||10-AUG-04
31375|Yeneena Supergroup|50544|5|Briefly described|p11|Neoproterozoic|Mesoproterozoic|Comprises the Throssell and Lamil Subgroups.  Geological Province: Yeneena Basin.||||||
31375|Yeneena Supergroup|50555|5|Briefly described|Map legend||Paleoproterozoic|Includes the Throssell and Lamil Groups.  Age: 1060 - 800Ma. Geological Province: Yeneena Basin.||||||07-NOV-08
31375|Yeneena Supergroup|60470|5|Briefly described|p2|Neoproterozoic|Neoproterozoic|upgraded from Yeneena Group (Bagas et al. 1995). Includes Throssell Range and Lamil Groups.Age uncertain. Deformed by Miles Orogeny ~720 Ma||||||
31375|Yeneena Supergroup|61272|6|Mentioned|p124|||||||||
31375|Yeneena Supergroup|64943|4|Described|p1, 2, 3 Fig. 1, p5, 13-14,19,  26, 29|Neoproterozoic|Mesoproterozoic|Defined by Bagas et al. (1995), to replace (part of) Yeneena Group. Includes Throssell and Lamil Groups. Four phases of metamorphism. Unconformably overlies Rudall Complex. Max age: 1333 Ma from Rb-Sr isochron on orthogneiss of Rudall Complex.||||||
31375|Yeneena Supergroup|65403|5|Briefly described|p13, p1, p5, p18, p20, pp26-29.|Neoproterozoic|Mesoproterozoic|Redefined; formerly Yeneena Group (Williams et al. 1976).|||Includes Throssell and Lamil Groups.|||29-SEP-15
31375|Yeneena Supergroup|65454|6|Mentioned|p30 Fig.A1b|Neoproterozoic|Neoproterozoic|Of Yeneena Basin||||||
31375|Yeneena Supergroup|67202|5|Briefly described|p4, p183, p185, p189, p196-197|||Up to c.13 km thick. Hosts the Magnum Au deposit (described), within or near the margins of a 250m thick gabbro body. Potential to host more unconformity-style uranium deposits.|||Throssell Group.|Is intruded by the O'Callaghans Supersuite.|Interlayered pelitic metasandstone and metasiltstone; upper greenschist facies.|
31375|Yeneena Supergroup|69185|5|Briefly described|500k_interpgeop_pilcrat02_lut.csv|||Of Yeneena Basin.|||Includes Throssell Group.|||
31375|Yeneena Supergroup|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, conglomerate, siltstone, crystalline dolostone/dolomite|
30329|Yenyening Formation|22769|3|Fully described|p763-64,Table3p764||Miocene|Middle unit of Salt River Group. Comprises mainly lake deposits formed of greenish to greyish clay with layers of blackish mudstone; two layers of lignite have been encountered in well drill cores.||||||17-JAN-06
30329|Yenyening Formation|65194|5|Briefly described|p123-125|Pliocene|Miocene|Salt River Palaeovalley sequence; unit in Salt River Group. Misspelt as Yenyenning repeatedly in text. Only known from drilling. Overlain by the (undated) South Caroline Clay. Green to grey clay and sandy clay, lignite, with inter-layered black mudstone and organic deposits which contain fossil leaves and branches. Lacustrine deposit.||||||
78996|Yilgaddy Andesite Member|70226|5|Briefly described|Map legend.|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Carton.||Yalgoo Formation|||Andesite to basaltic andesite; typically glassy and with distinctive coarsely spherulitic flows; minor basalt and dacite; metamorphosed. Includes felsic schist and andesitic volcanic breccia to sandstone; metamorphosed.|16-DEC-15
78996|Yilgaddy Andesite Member|70796|5|Briefly described|100k_geologyl_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv,  500k_interpgeop_lut.csv, Yalgoo100_2241_stratig.pdf. Numerous additional lithologies are discussed.|ca 2790  2760 Ma (inferred)|Yalgoo Formation|||Andesite to basaltic andesite; typically glassy and with distinctive coarsely spherulitic flows; minor basalt and dacite; metamorphosed. Felsic schist derived from andesitic to rhyolitic rocks; locally strongly deformed and sericiterich.|
78996|Yilgaddy Andesite Member|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.|2790-2760 Ma|Unit of Yalgoo Formation.|||Andesite to basaltic andesite; typically glassy and with distinctive coarsely spherulitic flows; minor basalt and dacite; metamorphosed; felsic schist derived from andesitic to rhyolitic rocks; locally strongly deformed and sericite-rich|
37193|Yilgatherra Formation|23525|4|Described|p29|Mesoproterozoic|Paleoproterozoic|Of the Edmund Group. Geological Province: Edmund Basin.||||||07-NOV-08
37193|Yilgatherra Formation|23527|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Edmund Group, Edmund Basin.||||||12-SEP-07
37193|Yilgatherra Formation|24115|4|Described|p4 Fig.2|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group. Maximum Thickness: ?<50m. Overlain by the Irregully Formation. Geological Province: Edmund Basin.||||||
37193|Yilgatherra Formation|24183|2|Defined|p7|Calymmian|Statherian|Max. Thickness: 350m. Unconformably overlies the Gascoyne Complex, Ashburton & Capricorn Formations. Conformably overlain by the Irregully Formation. Age: 1620-1462 Ma.||||||21-MAR-11
37193|Yilgatherra Formation|24544|5|Briefly described|p43, 44 Fig.32|Mesoproterozoic|Mesoproterozoic|Of Edmund Group. Overlain by Irregully Formation.||||||
37193|Yilgatherra Formation|50225|3|Fully described|p387 Fig. 2, p390|||Lowermost unit of Edmund Gp. Polymictic conglomerate, quartz sandstone + siltstone. Max. thick: 300m locally. Overlain by Irregully Fm; unconformably overlies Asburton Fm and Capricorn Gp, + some of the Gascoyne Complex rocks.||||||07-FEB-11
37193|Yilgatherra Formation|50292|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: <1620Ma. Geological Province: Edmund Basin. Of the Edmund Group (Bangemall Supergroup). Underlies: Irregully Formation.||||||07-NOV-08
37193|Yilgatherra Formation|50312|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group. Age: c. 1640 Ma. Overlain by Irregully Formation. Geological Province: Edmund Basin. Sandstone, siltstone and conglomerate.||||||07-NOV-08
37193|Yilgatherra Formation|50313|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup).  Geological Province: Edmund Basin. Age: c. 1640Ma.||||||07-NOV-08
37193|Yilgatherra Formation|60301|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin. Sandstone, conglomerate, siltstone and dolostone.||||||07-NOV-08
37193|Yilgatherra Formation|63470|5|Briefly described|Map legend||Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin. Sandstone, siltstone, conglomerate and dolostone.||||||07-NOV-08
37193|Yilgatherra Formation|63471|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup).Overlies Mount Augustus Sandstone; overlain by Irregully Formation.  Age: c.1620Ma. Geological Province: Edmund Basin. Sandstone, siltstone, conglomerate, and dolostone (section only).||||||07-NOV-08
37193|Yilgatherra Formation|63866|5|Briefly described|p162|||SHRIMP U-Pb zircon ages are detrital and according the author the age of this formation is constrained by its relationship with granites in the region which suggest a maximum depositional age of 1620 Ma. An additional age of 1685 +/- 33 Ma is derived from GSWA, 169093.|1805 +/- 9 Ma (Nelson, 2000) |Edmund Group||||
37193|Yilgatherra Formation|63869|5|Briefly described|p28-29, p53, Plate 1|Calymmian|Statherian|Martin and Thorne (2002). 300-350 m thick. Ages from underlying and intruding units.|c.1620-c.1465 Ma.|Basal unit in Edmund Group.||Unconformably overlies Ashburton Formation and Capricorn Group. Is overlain conformably by Irregully Formation.|Basal sandstone and conglomerate, overlain by siltstone and dolostone.|
37193|Yilgatherra Formation|64287|4|Described|p32, p34 Fig. 2|||Previously Yilgatherra Member of the Irregully Formation. Coarse-grained sandstone, siltstone, minor conglomerate. On EDMUND sheet.||||||07-FEB-11
37193|Yilgatherra Formation|64580|4|Described|map legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group. Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, sandstone, siltstone, and conglomerate.||||||15-DEC-08
37193|Yilgatherra Formation|64728|5|Briefly described|pp95-97, pp99-102. |Mesoproterozoic|Mesoproterozoic|Fluvial to shallow marine siliciclastic and carbonate facies. Highly variable paleocurrent directions.|Contains detrital zircons clustered  c.1800 Ma.|Unit in Edmund Group.||Unconformably overlies Paleoproterozoic basement. Is overlain by Irregully Formation.|Medium- to coarse-grained quartz sandstone; accessory tourmaline.|
37193|Yilgatherra Formation|65450|6|Mentioned|p5 Fig.2|Mesoproterozoic|Mesoproterozoic|||Edmund Group||||
37193|Yilgatherra Formation|65453|5|Briefly described|map legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group. Under Irregully Formation; over Moorarie Supersuite and Leake Spring Metamorphics. Age: < c. 1620 Ma. Sandstone; subordinate silstone, conglomerate and dolostone. Geol. Prov: Edmund Basin.||||||
37193|Yilgatherra Formation|65545|5|Briefly described|Map Legend|Mesoprotoerozoic|Paleoproterozoic|Of Edmund Group, Edmund Basin. Age: c. 1460 - <1620 Ma. Sandstone; subordinate siltstone, conglomerate, and dolostone.||||||
37193|Yilgatherra Formation|65549|5|Briefly described|Map Legend|Calymmian|Statherian|Of Edmund Group, Bangemall Supergroup, Edmund Basin. Underlies Irregully Formation; overlies rocks of the Gascoyne province. Age <1620Ma. Sandstone, subordinate siltstone, conglomerate, and dolostone.||||||06-SEP-10
37193|Yilgatherra Formation|65830|4|Described|p4, p9, p18, p19, p21-23; Plates 1,2|Calymmian|Statherian|Up to 350m thick. Basal Edmund Group. Fluvial to shallow-marine siliciclastic. Likely a partial correlative of the Mount Augustus Sandstone. Paleocurrent direction is down dip to the south west.||Of the Edmund Group||Overlain conformably by the Irregully Formation. Underlain by the Gascoyne Province. ?Intruded by the Durlacher Supersuite.|Consists of an upward-fining succession, from localised pebble to cobble conglomerate, through very coarse grained sandstone, to fine-grained sandstone and siltstone.|
37193|Yilgatherra Formation|66105|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin. Unit in Edmund Group. Under Irregully Formation; unconformably overlies Moorarie Supersuite and Leake Spring Metamorphics. Age: <1620 Ma. Sandstone; subordinate siltstone, conglomerate and dolostone.  ||||||
37193|Yilgatherra Formation|66110|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in Edmund Group. Sandstone, subordinate siltstone, conglomerate and dolostone.||||||
37193|Yilgatherra Formation|66112|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in Edmund Group. Age c.1620 Ma. Sandstone; subordinate siltstone, conglomerate and dolostone.||||||
37193|Yilgatherra Formation|66241|6|Mentioned|pp1-4. |||||Unit in Edmund Group.||Is overlain conformably by Irregully Formation.||
37193|Yilgatherra Formation|66299|4|Described|p51, p179, p236.|Mesoproterozoic|Mesoproterozoic|||Basal unit in Edmund Group.||Unconformably overlies Halfway Gneiss, a metagranodiorite unit of Moorarie Supersuite, and a Pooranoo Metamorphics gneiss.|Includes sandstone.|
37193|Yilgatherra Formation|66579|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin||Unit in Edmund Group.|||Sandstone; subordinate siltstone, conglomerate and dolostone.|
37193|Yilgatherra Formation|66887|5|Briefly described|p7|||||Edmund Group||Overlies Halfway Gneiss in Limejuice Zone.||15-DEC-16
37193|Yilgatherra Formation|67245|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Edmund Basin.||Unit in Edmund Group.||Overlies Moorarie Supersuite. Is overlain by Irregully Formation.|Sandstone, subordinate siltstone, conglomerate and dolostone; psammitic schist; quartz-feldspar-muscovite schist.|
37193|Yilgatherra Formation|67246|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Unit in Edmund Group.||Overlies nonconformably the Moorarie Supersuite. Is overlain by Irregully Formation.|Sandstone, subordinate siltstone, conglomerate and dolostone; thick-bedded conglomerate and sandstone.|19-NOV-13
37193|Yilgatherra Formation|67247|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Edmund Basin. Shown as part of 'Depositional package 1' in the interpreted bedrock geology map legend.|<1620 Ma.|Unit in Edmund Group.|||Sandstone; subordinate siltstone, conglomerate and dolostone.|20-NOV-13
37193|Yilgatherra Formation|67346|6|Mentioned|p795 Fig.2|Mesoproterozoic|Mesoproterozoic|||Of the Edmund Group.||||11-MAY-12
37193|Yilgatherra Formation|67371|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Edmund Basin.|<1620 Ma.|Unit in Edmund Group.|||Sandstone; subordinate siltstone, conglomerate and dolostone.|
37193|Yilgatherra Formation|67888|6|Mentioned|p96|||||||||
37193|Yilgatherra Formation|68522|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin.|<1620 - c.1465 Ma|Of the Edmund Group.|||Sandstone; subordinate siltstone, conglomerate and dolostone.|
37193|Yilgatherra Formation|69003|5|Briefly described|p34|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||Edmund Group.||Overlies Durlacher Supersuite nonconformably. Is overlain by Irregully Formation.||
37193|Yilgatherra Formation|69024|5|Briefly described|Map Legend|Statherian|Statherian|Edmund Basin.|c. 1620 Ma (Nelson, 1998)|Of the Edmund Group.||Overlain by the Irregully Formation.|Sandstone, siltstone, conglomerate and dolostone.|05-MAY-14
37193|Yilgatherra Formation|69027|5|Briefly described|Map Legend|Statherian|Statherian|Edmund Basin.|c. 1620 Ma (Nelson 1998)|Of the Edmund Group.||Underlain by the Ashburton Formation. Overlain by the Irregully Formation.|Sandstone, siltstone, conglomerate, and dolostone.|05-MAY-14
37193|Yilgatherra Formation|69028|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin. Mapped with Irregully Formation as one unit.||Of the Edmund Group.|||Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, sandstone, siltstone, and conglomerate.|06-MAY-14
37193|Yilgatherra Formation|69166|4|Described|geologyp_lut.csv|Mesoproterozoic|Paleoproterozoic|Age derived from sample of quartz sandstone (169093.1.pdf)|1685 Ma +/- 33 Ma (SHRIMP)|Edmund Group||Conformably overlain by Irregully Formation|Psammitic schist; quartz--feldspar--muscovite schist. Thickly bedded conglomerate, sandstone and siltstone, conglomerate and dolostone.|
37193|Yilgatherra Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|||Part of Edmund Group, Depositiional package 1.||Unit of Edmund Group.||||
37193|Yilgatherra Formation|69583|5|Briefly described|Plate 3|Mesoproterozoic|Mesoproterozoic|Edmund Basin.||Edmund Group.||||
37193|Yilgatherra Formation|69596|6|Mentioned|p12 Fig.7|||Edmund Basin.||Edmund Group.||||
37193|Yilgatherra Formation|70019|5|Briefly described|p93,108-109|Mesoproterozoic|Mesoproterozoic|Geological province: Gascoyne Province, Capricorn Orogen.||Unit of Edmund Group.|Includes Mount Augustus Sandstone.|Overlain by Irregully Formation. Underlain by Paleoproterozoic basement.||
37193|Yilgatherra Formation|70127|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin. An un-named sub-unit of siltstone with minor dolomitic siltstone and sandstone is mapped separately.||Edmund Group.|||Sandstone; subordinate siltstone, conglomerate and dolostone.|
37193|Yilgatherra Formation|70138|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Edmund Group.||Overlies Pooranoo Metamorphics. Is overlain by Irregully Formation.|Sandstone; subordinate siltstone, conglomerate and dolostone.|
37193|Yilgatherra Formation|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|100k_interpgeop_lut.csv, 169093.1.pdf, West Australian Craton, Edmund Basin|1679-1610 Ma|Edmund Group||Conformably overlain by Irregully Formation, Fluvial facies may correlate with Mount Augustus Sandstone, Overlies Mount Augustus Sandstone, Labouchere Formation, Intruded by Waldburg Dolerite|Psammitic schist, thick bedded conglomerate and sandstone, siltstone, quartz sandstone; minor dolomitic siltstone.|
37193|Yilgatherra Formation|70814|4|Described|p3, p5, p7-p8, p20, p22, p24-p25, p53|Statherian|Statherian|Edmund Basin. Together with the Irregully Formation forms Depositional Package 1 of the Edmund Group. This unit fines upwards. This formation is thin and discontinuous in the Pingandy Shelf area but on the Pink Hills and Candolle map sheets this unit reaches its maximum thickness of 550m. Lithology in different areas are described. Age is derived from the maximum age of the underlying Mount Augustus Sandstone. Overlain by the Irregully Formation. Intruded by the Waldburg Dolerite.|1679-1610 Ma|Edmund Group||Unconformably overlies the Wyloo, Capricorn and Padbury Groups. Unconformably overlies (or is faulted against) the Mount Augustus Sandstone.|Shallow-marine to fluvial conglomerate and sandstone overlain by deeper marine siltstone.|
37193|Yilgatherra Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolostone, siltstone, sandstone, conglomerate, crystalline dolostone/dolomite|
37193|Yilgatherra Formation|71273|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin.||Edmund Group.|||Sandstone; subordinate siltstone, conglomerate and dolostone. (Separately mapped) thick-bedded conglomerate and sandstone; siltstone, minor dolomitic siltstone and sandstone.|
37193|Yilgatherra Formation|72705|5|Briefly described|p3-5|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.|<1679 Ma (U-Pb detrital zircon).|Edmund Group.||Is overlain conformably by Irregully Formation. Correlative of Mount Augustus Sandstone.|Fluvial to shallow marine sandstone and siltstone.|
37193|Yilgatherra Formation|73442|6|Mentioned|p8|||Also referred to as Depositional Package 1.||||Intruded by Waldburg Dolerite||
35656|Yilingbun Granophyre|23125|4|Described|Table.1, p388||Proterozoic|Age: Early Proterozoic. New name given to granpohyric phase of the Hart Dolerite.||||||
78385|Yilmia Gabbro|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2696 Ma (inferred).|Leviathan Suite|||Gabbro to pyroxenite; metamorphosed. Orthopyroxenite, pyroxene bearing peridotite; metamorphosed.|
78385|Yilmia Gabbro|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2696 Ma (inferred)|Unit of Leviathan Suite.|||Gabbro to pyroxenite; metamorphosed; Orthopyroxenite and pyroxene-bearing peridotite; metamorphosed|
29194|Yilmia sill|30900|5|Briefly described|p70|||||||||
29194|Yilmia sill|43102|5|Briefly described|Fig.3|||||||||
26248|Yoganup Formation|12759|5|Briefly described|p43-7; p28 Tb. 7; p32 Fig 15; P36 Fig 17|Quaternary||Defined Low (1971). Type section: open cut sand mine near Yoganup, 200 km S of Perth (AMG Zone 50, 370433m E, 6276070m N).  Max thickness is 10m.||Unit in Kwinana Group.||Unconformable on Osborne or Leederville Formations. Is overlain unconformably by Guildford Clay.|Unconsolidated, poorly sorted sand, gravel and pebbles with local subordinate clay, ferruginized grains and heavy minerals.|12-MAY-14
26248|Yoganup Formation|14227|5|Briefly described|Enclos. 2|Pliocene|Pliocene|Presented as Yoganup Fm.||||||07-FEB-11
26248|Yoganup Formation|23816|6|Mentioned|p256|||Max. thickness: 10 m.||||||
26248|Yoganup Formation|24410|5|Briefly described|p39|Quaternary|Quaternary|Of the Kwinana Group. Shoreline deposit consisting of basal conglomerate and foredune containing discontinuous concentrations of heavy minerals together with leached quartz sand. Geological Province: Perth Basin.||||||24-NOV-09
26248|Yoganup Formation|24464|5|Briefly described|p332 Fig. 1|||||||||
26248|Yoganup Formation|29693|6|Mentioned|p41|||||||||
26248|Yoganup Formation|30217|5|Briefly described|p21|||||||||
26248|Yoganup Formation|30939|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
26248|Yoganup Formation|31896|2|Defined|p34|middle Pleistocene|middle Pleistocene|Probably Middle Pleistocene.||||||14-FEB-08
26248|Yoganup Formation|33044|4|Described|p57|||See also map 3 and 4 and Diagram 17.||||||17-JAN-08
26248|Yoganup Formation|33747|5|Briefly described|p1071|||||||||
26248|Yoganup Formation|35058|6|Mentioned|p64|||||||||
26248|Yoganup Formation|35638|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
26248|Yoganup Formation|36293|3|Fully described|p208|||||||||
26248|Yoganup Formation|36890|5|Briefly described|p256|||||||||
26248|Yoganup Formation|37017|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
26248|Yoganup Formation|38775|4|Described|p43|||||||||
26248|Yoganup Formation|38997|4|Described|p8|||||||||
26248|Yoganup Formation|39554|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
26248|Yoganup Formation|39829|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
26248|Yoganup Formation|39915|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
26248|Yoganup Formation|40304|5|Briefly described|p42|||||||||
26248|Yoganup Formation|40359|5|Briefly described|p28|||||||||
26248|Yoganup Formation|40360|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
26248|Yoganup Formation|41251|4|Described|p36|||||||||
26248|Yoganup Formation|41344|6|Mentioned|p208|||||||||
26248|Yoganup Formation|41346|6|Mentioned|p170|||||||||
26248|Yoganup Formation|41504|6|Mentioned|p71|||||||||
26248|Yoganup Formation|41782|4|Described|p24|||||||||
26248|Yoganup Formation|41783|4|Described|p45|||||||||
26248|Yoganup Formation|41831|6|Mentioned|p556|||||||||
26248|Yoganup Formation|41912|6|Mentioned|p31|||||||||
26248|Yoganup Formation|41986|3|Fully described|p34|||||||||
26248|Yoganup Formation|42009|6|Mentioned|p75|||||||||
26248|Yoganup Formation|42687|6|Mentioned|map legend|||||||||
26248|Yoganup Formation|42688|6|Mentioned|map legend|||||||||
26248|Yoganup Formation|43062|5|Briefly described|p23,Table 2,p18|||||||||
26248|Yoganup Formation|43189|5|Briefly described|Map Legend||Quaternary|||||||
26248|Yoganup Formation|43197|5|Briefly described|Map Legend||Tertiary|||||||
26248|Yoganup Formation|43212|5|Briefly described|p6||Pleistocene|||||||
26248|Yoganup Formation|43306|5|Briefly described|Map Legend||Quaternary|||||||
26248|Yoganup Formation|43308|5|Briefly described|Map Legend||Quaternary|||||||
26248|Yoganup Formation|43309|5|Briefly described|Map Legend||Quaternary|||||||
26248|Yoganup Formation|43347|5|Briefly described|10||Pliocene|||||||
26248|Yoganup Formation|44144|4|Described|p502 Tb.4-21, p520|Cenozoic|Cenozoic|Type Section: near Yoganup; 33o38'50''S 115o36'10''E.  6-9 m of unfossiliferous shoreline deposits.|||||Sand and lenticular clay beds, with basal conglomerate.|
26248|Yoganup Formation|50621|5|Briefly described|p165 Fig. 6|Quaternary|Quaternary|Geological Province: Perth Basin.||||||13-AUG-04
26248|Yoganup Formation|60556|5|Briefly described|p22, p25 Fig. 15, p34|||||||||
26248|Yoganup Formation|61155|5|Briefly described|p5|Pliocene|Pliocene|With siliciclastic facies; contains heavy minerals. Overlies and interfingers with Ascot Beds; laterally interfingers with Wadjemup Formation. Thickness: 6m. Geological Province: Perth Basin.||||||
26248|Yoganup Formation|62369|6|Mentioned|p414|||Includes the Jandakot Member. Geological Province: Perth Basin.||||||
26248|Yoganup Formation|63745|5|Briefly described|p61, p62 Fig. 2|Pliocene|Pliocene|Unconformably overlain by Guildford Formation. Includes conglomerates and sand.||||||07-FEB-11
26248|Yoganup Formation|67135|6|Mentioned|p64, p65 Fig.88.|||Source of sand, mainly for construction.||||||
26248|Yoganup Formation|68811|5|Briefly described|p90, p94|Quaternary|Neogene|One of a group of 'superficial sediments' described as being up to 90m thick. .|||||Group description: Sand, limestone, silt and clay.|15-APR-20
26248|Yoganup Formation|70097|5|Briefly described|p19 Fig.3|Pliocene|Miocene|Southern Perth Basin. Beermullah Trough, Mandurah Terrace and Bunbury Trough.||||Overlies Warnbro Group or Kings Park Shale. Is overlain by Tamala Limestone or Bassendean Sandstone.|Sandstone.|13-SEP-17
26248|Yoganup Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sand, eolian, coastal sediment, conglomerate|
26248|Yoganup Formation|71377|5|Briefly described|p7|Quaternary|Neogene|Perth Basin.||||||
78359|Youangarra Volcanics Member|70140|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. 15 facies are mapped separately.|c.2814 Ma.|Yaloginda Formation.|||Metamorphosed siliciclastic rocks interlayered with felsic schist; local dacitic lava; minor metachert and metamorphosed BIF; locally strongly sheared.|
78359|Youangarra Volcanics Member|70796|5|Briefly described|100k_geologyl_lut.csv|Neoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, Youanmi100_2640_stratig.pdf. Numerous additional lithologies are discussed.|ca 2815 to 2800 Ma (inferred)|Yaloginda Formation|||Metamorphosed banded ironformation; Metamorphosed banded chert interlayered with psammitic rocks and minor felsic schist and metavolcaniclastic rocks.|
78359|Youangarra Volcanics Member|71269|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeol_lut.csv.|2815-2800 Ma|Unit of Yaloginda Formation.|||Metamorphosed siliciclastics interlayered with felsic schist; dacitic lava to volcaniclastics; minor metachert and metamorphosed BIFs; locally sheared; quartzitic schist, metamorphosed banded chert, porphyritic dacite, mafic schsits, andesite flows|
74842|Youanmi Igneous Complex|44149|6|Mentioned|p120 Fig.2-125|||Appears as Youanmi Complex.||||||
74842|Youanmi Igneous Complex|64891|5|Briefly described|p37 Fig. 2, p50-51 Tb. 1|Archean|Archean|Of the Meeline Suite. Age. c. 2780Ma. Geological province: Murchison Domain. Layered gabbro and anorthosite with magnetite and pyroxenite layers, and thick ultramafic accumulates; metamorphosed.||||||07-FEB-11
74842|Youanmi Igneous Complex|66195|4|Described|p604, 605, 598, p599 Fig.2, p601, 602|Neoarchean||Intrudes altered felsic volcanic rocks with crystallisation age of 2814+/-14 Ma. >4km thick, divided into lower zone (~2km thick), main zone (~3.5km thick) and upper zone (~500m thick). For more detail see figure 4||In Meeline Suite.||||13-MAR-12
74842|Youanmi Igneous Complex|67129|6|Mentioned|p18 Fig.19, p51-52, p54, p56-57|||Murchison Domain, Youanmi Terrane.|c.2810 Ma.|Meeline Suite.||||07-SEP-17
74842|Youanmi Igneous Complex|68561|5|Briefly described|GEOCHRON files|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane. Dolerite U-Pb zircon age: 2825 +/- 7 Ma tentatively interpreted as the age of an older source rock from which the zircons were derived, and therefore as a maximum age for the magmatic crystallization of the dolerite. Geochron file 194751.1.pdf.  Intrudes strongly altered felsic volcanic host rocks, interpreted to have crystallized at 2814 +/- 14 Ma (GSWA 169067, Nelson, 2002). See geochron file 194747.1.pdf.||Meeline Suite||||
74842|Youanmi Igneous Complex|69583|5|Briefly described|p49-50, p55-56, p98, p100-102, p176-177|Mesoarchean|Mesoarchean|See also Plate 2. Murchison Domain, Youanmi Terrane, Yilgarn Craton. Mineralisation style, geochronological data, igneous stratigraphic column. The four zones are mapped separately. Age appears anomalously as 2919 Ma on p102 and p177. Shows indications of Ni-Cu sulfide mineralisation.|2819 Ma.|Meeline Suite.|||Dolerite; modally layered pyroxenitic gabbro interlayered with serpentinite; gabbronorite grading into norite and leucogabbronorite, interlayered with gabbro; magnetitite interlayered with modally layered magnetite-bearing leucogabbro; metamorphosed.|
74842|Youanmi Igneous Complex|69584|6|Mentioned|p2|Mesoarchean|Mesoarchean||2825 +/- 7 Ma (U-Pb zircon)|Meeline Suite||||
74842|Youanmi Igneous Complex|69586|5|Briefly described|p22|Mesoarchean|Mesoarchean|Murchison Domain.||Meeline Suite.||||
74842|Youanmi Igneous Complex|70140|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Comprises 23 un-named facies mapped separately, but grouped into Border, Ultramafic, Lower, Middle and Upper zones.|2819 Ma (Gill, 2011 unpublished).|Meeline Suite.|||Border zone: dolerite. Ultramafic zone: ultramafic layered cumulate rocks. Lower zone: gabbro; gabbronorite, norite. Middle zone: leucograbbro, pyroxenite, magnetite cumulate. Upper zone: dolerite, gabbro, mafic schist. All metamorphosed.|
74842|Youanmi Igneous Complex|70332|5|Briefly described|p77-81, 83-84|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|c.2818 Ma (Gill, 2011).|Meeline Suite.|||Includes one observed hornblende gabbro layer.|
74842|Youanmi Igneous Complex|70419|5|Briefly described|p1-3, p7-9, p11|Mesoarchean|Mesoarchean|Referred to as YIC throughout. Comprises a middle and an upper zone. Possibly could have been part of the Windimurra Igneous Complex, now separated by 12-32 km width of granitic plutons.|2919 Ma (Gill, 2011).|Meeline Suite.||||
74842|Youanmi Igneous Complex|70796|4|Described|2_5m_interpgeop15_lut.csv|Mesoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. Affected by the Yilgarn Craton granite magmatism (3010  2600 Ma); Youanmi Terrane events (3131  2600 Ma). See also 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 194751.1.pdf. Numerous additional lithologies are provided. |ca 2819 Ma (inferred)|Meeline Suite|||Layered gabbro and leucogabbro with magnetitite and pyroxenite layers; metamorphosed. Tremolite rich ultramafic schist.|
74842|Youanmi Igneous Complex|70830|5|Briefly described|p4, p27, p29, p55|||||Meeline Suite||||
74842|Youanmi Igneous Complex|71168|5|Briefly described|p7, p18, p20-p21|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c. 2800 Ma|Meeline Suite||||
74842|Youanmi Igneous Complex|71311|6|Mentioned|p794|||Northern Youanmi Terrane, Yilgarn Craton.||||||
74842|Youanmi Igneous Complex|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Youanmi Terrane. 4 unnamed subdivisions shown. Upper,  middle, lower and border zones.||Youanmi Igneous Complex|||Magnetitite interlayered w modally layered magnetite-bearing leucogabbro. Gabbronorite interlayered w gabbro on 50 m scale; contacts locally gradational. Modally layered pyroxenitic gabbro interlayered w serpentinite. Dolerite. All metamorphosed.|
78358|Yuinmery Volcanics Member|69584|6|Mentioned|p6|Mesoarchean|Mesoarchean|||Yaloginda Formation||||
78358|Yuinmery Volcanics Member|70140|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. 7 facies are mapped separately.||Yaloginda Formation.|||Felsic schist with local dacite to rhyolite lava, interlayered with metamorphosed BIF; locally strongly sheared.|
78358|Yuinmery Volcanics Member|70796|5|Briefly described|100k_geologyl_lut.csv|Neoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, Youanmi100_2640_stratig.pdf. Numerous additional lithologies are discussed.|ca 2815 to 2800 Ma (inferred)|Yaloginda Formation|||Metamorphosed banded ironformation; typically with coarse, granular, recrystallized magnetite crystals; commonly foliated.|
78358|Yuinmery Volcanics Member|71269|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.|2815-2800 Ma|Unit of Yaloginda Formation.|||Felsic schist with local dacite-rhyolite lava, interlayered with metamorphosed banded iron-formation; locally strongly sheared; rhyolitic schists, porphyritic dacite, mafi schists.|
32788|Yungul carbonatite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Informal name.  Calcite-apatite-anatase rock.  Age: <1790Ma.||||||07-NOV-08
32788|Yungul carbonatite|44230|5|Briefly described|Map Legend||Proterozoic|||||||
26251|Yurabi Formation|22764|4|Described|Table1,p6||Adelaidean|Louisa Downs Group. 320 m. Conformable on Egan Formation, unconformable on Olympio Formation.||||||01-FEB-10
26251|Yurabi Formation|23383|4|Described|p21, p18 Tb. 2|Neoproterozoic|Neoproterozoic|Of Louisa Downs Gp.  Quartz sst. interbedded with sltst., mudst., laminated dolomitic sltst., and silty or sandy dolomite.  Conformably overlain by McAlly Shale; disconformably underlain by Egan Fm. Max. thickness: 100 m.  Geol.Prov: Louisa Basin.||||||25-JAN-05
26251|Yurabi Formation|23599|4|Described|p18|Neoproterozoic|Neoproterozoic|Of Louisa Downs Group. Overlying unit McAlly Shale. Underlying unit Egan Formation. Geological Province: Louisa Basin. Max. thickness: 125 m.||||||
26251|Yurabi Formation|23601|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Louisa Downs Group. Flaggy to blocky quartz sandstone and feldspathic sandstone; grey and purple siltstone, shale, dolomitic siltstone, and sandy dolomite.||||||25-JAN-05
26251|Yurabi Formation|23806|5|Briefly described|p1122|||||||||
26251|Yurabi Formation|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26251|Yurabi Formation|32660|5|Briefly described|Table 6|||||||||
26251|Yurabi Formation|32728|6|Mentioned|Table 7|||||||||
26251|Yurabi Formation|35120|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26251|Yurabi Formation|36048|6|Mentioned|p381|||||||||
26251|Yurabi Formation|36551|6|Mentioned|Table 10|||||||||
26251|Yurabi Formation|36888|4|Described|p214|||||||||
26251|Yurabi Formation|36898|5|Briefly described|Table IV|||See also Fig.2B||||||
26251|Yurabi Formation|37927|6|Mentioned|p506|||||||||
26251|Yurabi Formation|38157|6|Mentioned|Table X|||||||||
26251|Yurabi Formation|41429|6|Mentioned|p247|||||||||
26251|Yurabi Formation|44140|4|Described|p301 fig 4-7, p303 Tb.4-2|Neoproterozoic|Neoproterozoic|Of Mount Ramsay area. 30-210 m thick. Probably equivalent to Mount Forster Sandstone, Elvire Formation and Boonall Dolomite (i.e. lower Albert Edward Group).||Louisa Downs Group||Conformably overlies Egan Formation. Is overlain conformably by McAlly Shale.|Quartz sandstone and feldspathic quartz sandstone; interbedded shale, siltstone and dolomitic beds.|08-MAR-18
26251|Yurabi Formation|44231|5|Briefly described|Map Legend||Proterozoic|Of the Louisa Downs Group. Flaggy to blocky quartz sandstone and feldspathic sandstone; grey or purple siltstone, shale, dolomitic siltstone, and sandy dolomite. Geological Province: Louisa Basin.||||||26-MAY-05
26251|Yurabi Formation|44398|14|Not recorded|map legend||Adelaidean|||||||
26251|Yurabi Formation|44693|5|Briefly described|Map Legend||Proterozoic|||||||
26251|Yurabi Formation|44694|5|Briefly described|Map Legend||Proterozoic|||||||
26251|Yurabi Formation|45047|4|Described|p36|||Louisa Downs Group.||||||
26251|Yurabi Formation|48927|2|Defined|p26|Adelaidean|Adelaidean|||||||
26251|Yurabi Formation|61574|5|Briefly described|p690|Neoproterozoic III|Neoproterozoic III|Of the Louisa Downs Group. Together with Egan Formation, unconformably overlies (locally) the Crowhurst Group.||||||07-JAN-10
26251|Yurabi Formation|63458|6|Mentioned|p873 Fig.2, p896 Fig.18, p897 Fig.19. |Ediacaran|Ediacaran|||Unit in Louisa Downs Group.||Overlies Egan Formation.||
26251|Yurabi Formation|67484|6|Mentioned|p294 Tb.1|Ediacaran|Ediacaran|Mount Ramsay area, West Kimberley. ||Of the Louisa Downs Group.||Overlies Egan Formation. Is overlain by McAlly Shale.||
26251|Yurabi Formation|67620|4|Described|p1-7, 11-13, 19-22|Ediacaran|Ediacaran|Mount Ramsay area, Kimberley region. Contains extremely abundant and exceptionally well-preserved microbially-induced sedimentary structures. Peritidal sediments; 45-55m thick. Detailed logged outcrop section. Sedimentary facies/associations described in great detail. Abundant photographs, SEM images.||Louisa Downs Group.||Conformably overlies Egan Formation. Is overlain by the McAlly Shale. Correlates with the Bonney Sandstone Formation (SA).|Sandstone and mudstone with minor interbeds of dolomicrite and dolostone.|
26251|Yurabi Formation|68138|6|Mentioned|p156|Neoproterozoic|Neoproterozoic|Mount Ramsay area, Kimberley region.||Louisa Downs Group.||||
26251|Yurabi Formation|68244|4|Described|p659-660,665|Neoproterozoic|Neoproterozoic|Louisa Basin, Kimberley region.||Unit of Louisa Downs Group.||Overlain by McAlly Shale. Underlain by Egan Formation.|Sandstone|
26251|Yurabi Formation|68473|6|Mentioned|p529-532, p534, p546-547|||Mount Ramsay. Part of the postglacial succession.||Louisa Downs Group||Equivalent to the lower part of the Timperley Shale.||
26251|Yurabi Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Cryogenian|Cryogenian|Louisa Basin||Louisa Downs Group|||Flaggy to blocky quartz sandstone and feldspathic sandstone; grey or purple siltstone, shale, dolomitic siltstone and sandy dolomite.|04-AUG-15
26251|Yurabi Formation|69165|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran||||||Flaggy to blocky quartz sandstone and feldspathic sandstone; grey or purple siltstone, shale, dolomitic silstone and sandy dolomite.|
26251|Yurabi Formation|69634|4|Described|100k_interpgeop_lut.csv|Cryogenian|Cryogenian|Geological province: Halls Creek Orogen. Of Louisa Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1.|850-635 Ma (Biostrat)|Unit of Louisa Downs Group.|||Flaggy to blocky quartz sandstone and feldspathic sandstone; grey or purple siltstone, shale, dolomitic siltstone and sandy dolomite|
26251|Yurabi Formation|70154|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran||541-635 Ma|Louisa Downs Group|||Flaggy to blocky quartz sandstone and feldspathic sandstone; grey or purple siltstone, shale, dolomitic siltstone and sandy dolomite|
26251|Yurabi Formation|71267|4|Described|GEOL_LUT_CSV files|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Louisa Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|635-541 Ma (biostrat)|Unit of Louisa Downs Group.|||Glacigenic, medium-bedded, moderately to poorly sorted, fine- to medium-grained, ripple-laminated quartz sandstone interbedded with siltstone, mudstone, laminated dolomitic siltstone, and silty or sandy dolomite.|
75591|Zeepaard Formation|6876|6|Mentioned|p100 Fig.5.|Early Cretaceous|Early Cretaceous|||||||
75591|Zeepaard Formation|12491|5|Briefly described|p448, p451, pp455-459.|||Valanginian to Hauterivian sediment sourced from Valanginian uplift of Barrow Group and older Jurassic sediments. Reservoir for Griffin Area fields hydrocarbons. Misspelt as Zeepard Formation in text on p448 and p450 Fig.3 caption.||||Overlies Barrow Group. Is overlain by Birdrong and Muderong Formations.||06-NOV-14
75591|Zeepaard Formation|61555|6|Mentioned|p241|||Absent in this area||||||
75591|Zeepaard Formation|67970|5|Briefly described|p10. |Early Valanginian|Early Valanginian|Exmouth Plateau.||||Is overlain by Birdrong Formation.|Delta-front sandstones.|
75591|Zeepaard Formation|69689|5|Briefly described|p16, 18|Cretaceous|Cretaceous|Exmouth Sub-basin, Northern Carnarvon Basin. A deltaic system building west and northwards from the Exmouth Sub-basin.||Upper Barrow Group.||Overlies Lower Barrow Group. Is overlain by Birdrong Formation.||05-APR-22
75591|Zeepaard Formation|70066|5|Briefly described|Regional: Fig.6; p6|Valanginian|Valanginian|Rankin Platform, Exmouth and Barrow Sub-basins, Northern Carnarvon Basin. Progradational top-set units.||Winning Group.||Overlies Barrow Group or Flag Sandstone. Is overlain by Muderong Shale and ?Birdrong Sandstone.||
75591|Zeepaard Formation|73564|5|Briefly described|p1223, 1225-1227, 1229-1233, 1235-1237|Cretaceous|Cretaceous|See also p1239. Gascoyne Margin. Possibly sourced from Barrow Group, uplifted at the Ningaloo Arch. A relatively thin (<300m thick) progradational deltaic sequence. This has also been defined as the Upper Barrow Group; but it formed after the Intra-Valanginian unconformity, in response to different uplift and subsidence processes, and is thus regarded as a separate unit. Palynology detailed.||||Overlies Barrow Group. Is overlain by Birdrong Sandstone.||
75513|Ziggy Monzogranite|66121|5|Briefly described|Map legend|Archean|Archean|Yamarna Terrane, Yilgarn Craton. Age c.2832 Ma. Medium- to coarse-grained, seriate-textured monzogranite; variably foliated and metamorphosed.||||||02-MAY-13
75513|Ziggy Monzogranite|68107|4|Described|p607 Fig.3, p608 Fig. 4, p609 Tb.1.|Mesoarchean|Mesoarchean|Dorothy Hills Greenstone Belt, Yamarna Terrane. A small, irregular body.|2832 +/- 4 Ma (Wingate et al. 2010).||||Variably foliated, seriate-textured monzogranite.|22-SEP-14
75513|Ziggy Monzogranite|69091|5|Briefly described|p179|||Ziggy Monzogranite possibly represents a surface expression of Babool Seismic Province. Magmatic crystallisation age by Pawley et al. (2012).|2832 +/- 4 Ma, SHRIMP U-Pb zircon|||||
75513|Ziggy Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Mesoarchean|Mesoarchean|Yilgarn Craton. Igneous crystallization age U/Pb SHRIMP. Sample described as metatonalite. See geochron file 179450.1.pdf (2010)|2832+/-4 Ma||||Medium- to coarse-grained, seriate-textured monzogranite; variably foliated and metamorphosed.|07-AUG-15
75513|Ziggy Monzogranite|69404|6|Mentioned|p4 Fig.4|Mesoarchean|Mesoarchean|Yamarna Terrane|c. 2825 Ma|||||
75513|Ziggy Monzogranite|70153|5|Briefly described|100k_interpgeop_lut.csv|Mesoarchean|Mesoarchean|See also 100k_geologyp14_lut.csv and 500k_interpgeop14_lut.csv. Age derived from equigranular to porphyritic tonalite sample (179450.1.pdf)|2832 +/- 4 Ma (SHRIMP)||||Medium- to coarse-grained, seriate-textured monzogranite; variably foliated and metamorphosed.|
75513|Ziggy Monzogranite|70802|5|Briefly described|500k_interpgeop14_lut.csv|Mesoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism.|2832+\-4 Ma||||Medium- to coarse-grained, seriate-textured monzogranite; variably foliated and metamorphosed|
75513|Ziggy Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). Sample GSWA 179450 (metatonalite) yielded a weighted mean 207Pb/206Pb date of 2832+\-5 Ma, interpreted to be igneous crystallisation age of the tonalite. See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 100k_geologyp14_lut.csv, 500k_interpgeop_lut.csv, 2_5m_interpgeop15_lut.csv.|2832+\-4 Ma||||Medium- to coarse-grained, seriate-textured monzogranite; variably foliated and metamorphosed|
75513|Ziggy Monzogranite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Yilgarn Craton.|2832+/-4 Ma.||||Medium- to coarse-grained, seriate-textured monzogranite; variably foliated and metamorphosed.|
39502|Zulu Granodiorite|63417|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite.  Age: 3299-3294Ma. Geological Province: Pilbara Craton. Biotite granodiorite, locally includes tonalite and monzogranite; medium- to coarse-grained, weakly foliated; metamorphosed.||||||07-NOV-08
39502|Zulu Granodiorite|63441|5|Briefly described|p8 Tb. 2|Archean|Archean|Of Emu Pool Supersuite. Ages: 3299+/-3Ma and 3294+/-5Ma. Geological province: Pilbara Craton.||||||07-FEB-11
39502|Zulu Granodiorite|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||Of Mount Edgar Granitoid Complex.|||Biotite granodiorite, tonalite and monzogranite; medium- to coarse-grained, weakly foliated; granitoid rock with mafic and ultramafic xenoliths.|
39502|Zulu Granodiorite|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|3299 - 3294 Ma.|Of Emu Pool Supersuite.|||Biotite granodiorite, local tonalite and monzogranite, medium- to coarse-grained, weakly foliated; granitic rock with numerous mafic and ultramafic xenoliths. All metamorphosed.|
39502|Zulu Granodiorite|65827|2|Defined|p6 Tb.2, p9 Fig 3, p13 Tb.4, p26, p57-58|Paleoarchean|Paleoarchean|New name. 26 x 6 km arcuate intrusion around Chimingadgi Hill. 3299+/-3 Ma (SHRIMP U-Pb zircon; Love et al. 2006) to 3294+/-5 Ma (SHRIMP U-Pb zircon; Nelson 2005).   Corresponds in part to Chimingadgi Suite; faulted against Kennell Granodiorite, Gorge Creek Group, Mount Roe Basalt, Hardey Formation, Cleaverville Formation. Appears as Zulu granodiorite on p58.  Hosts gold-bearing quartz veins at the Expectation mine.||Of Emu Pool Supersuite.||Intruded by Bishop Creek and Bullgarina Monzogranites; intrudes Mullugunya Granodiorite, Apex Basalt.|White to grey, seriate to even-grained, medium- to coarse-grained biotite granodiorite, tonalite and monzogranite.|21-MAY-14
39502|Zulu Granodiorite|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Age derived from sample of foliated monzogranite (178096.1.pdf)|3297 +/- 4 Ma (SHRIMP)|Emu Pool Supersuite|||Biotite granodiorite; local tonalite and monzogranite; medium to coarse grained, weakly foliated. Granodiorite with numerous mafic and ultramafic xenoliths.|
39502|Zulu Granodiorite|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA 178096 (biotite monzogranite) yielded an interpreted igneous crystallisation age of 3297+\-4 Ma for the monzogranite (weighted mean 207Pb/206Pb). Sample GSWA 178098 (biotite monzogranite) yielded an interpreted igneous crystallisation age of 3299+\-3 Ma for the monzogranite (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|3299-3294 Ma (inferred)|Unit of Emu Pool Supersuite.||Intruded by Bishop Creek Monzogranite and Bridget Suite.|Granodiorite and niotite granodiorite; local tonalite and monzogranite; medium to coarse grained, weakly foliated, numerous mafic and ultramafic xenoliths; metamorphosed.|
39502|Zulu Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite, tonalite, monzogranite|
39502|Zulu Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||Max age 3299+/-3 Ma, min 3294+/-5 Ma.|Emu Pool Supersuite|||Biotite granodiorite; local tonalite and monzogranite; medium to coarse grained, weakly foliated.|
30721|granite 30721|29811|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
35716|granite 35716|30954|6|Mentioned|Map legend|Archean|Archean|Granite with rare potassium feldspar phenocrysts.||||||07-NOV-08
35716|granite 35716|30959|6|Mentioned|Map legend|Archean|Archean|Granites: not subdivided - locally porphyritic, commonly foliated; unknown mutual relationships; abundant pegmatites in places.||||||07-NOV-08
35716|granite 35716|30975|6|Mentioned|Map legend|Archean|Archean|Unassigned granitic rock.||||||07-NOV-08
35716|granite 35716|42724|5|Briefly described|map legend|Archean|Archean|Granitoid rock.||||||07-NOV-08
36655|limestone 36655|23756|5|Briefly described|map legend|Eocene|Eocene|Tel. Limestone.||||||
36656|limestone 36656|23756|5|Briefly described|map legend|Miocene|Miocene|Tm (e>1) l. Limestone.||||||
36657|limestone 36657|23756|5|Briefly described|map legend|Miocene|Miocene|Tm (e>u) l. Limestone.||||||
36658|limestone 36658|23756|5|Briefly described|map legend|Miocene|Miocene|Tme. Limestone.||||||
36659|limestone 36659|23756|5|Briefly described|map legend|Miocene|Miocene|Tm (f>1-2) l. Limestone.||||||
36660|limestone 36660|23756|5|Briefly described|map legend|Miocene|Miocene|Tml Limestone -undifferentiated.||||||
36661|limestone 36661|23756|5|Briefly described|map legend||Miocene|Tm (?). Limestone. Age: Miocene or younger.||||||
36662|limestone 36662|23756|5|Briefly described|map legend|Quaternary|Tertiary|Tz. Limestone - undifferentiated.||||||
36663|limestone 36663|23756|5|Briefly described|map legend|Quaternary|Tertiary|Tzp. Pinnacles of limestone with variable amounts of Czp (unconsolidated phosphatic soil)||||||
35955|orthogneiss 35955|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Compositionally layered orthogneiss derived from fine to medium-grained granite or monzogranite; contains alternating biotite and feldspar-rich layers; local lenticular inclusions of metamorphosed mafic, ultramafic and sedimentary rocks. Rudall Complex.||||||
35956|orthogneiss 35956|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Biotite granodioritic orthogneiss.||||||
36669|pellet limestone 36669|23756|5|Briefly described|map legend|Recent|Recent|Czl. Pellet limestone, contains pellets and pebbles of phosphate rock||||||
36665|phosphate rock 36665|23756|5|Briefly described|map legend|Recent||P. Phosphate rock - massive boulder, and pebble deposits||||||
36670|phosphatic soil 36670|23756|5|Briefly described|map legend|Recent|Recent|Czp. Unconsolidated material - mostly phosphatic soil containing >20% P2O5||||||
36664|phosphatised "volcanics" 36664|23756|5|Briefly described|map legend|Quaternary|Tertiary|Pv. Phosphatised "volcanics".||||||
36671|talus 36671|23756|6|Mentioned|map legend|Quaternary|Quaternary|no map symbol. Talus.||||||
36654|volcanics 36654|23756|5|Briefly described|map legend|Tertiary|Tertiary|Tb. Volcanics - mostly basalt, some tuff, scoria, - undifferentiated.||||||
